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
21097|Aberdare Dolerite|23926|6|Mentioned|p19 Fig. 7|||||||||
21097|Aberdare Dolerite|23928|5|Briefly described|p70|||Geological Province: Yilgarn Craton.||||||
21097|Aberdare Dolerite|62108|5|Briefly described|p1420 Fig. 14|||In the Kalgoorlie district. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
21097|Aberdare Dolerite|65834|6|Mentioned|p53-54, 56|||Kalgoorlie Goldfield. Initially thought to be extension of Golden Mile Dolerite.||||||
21097|Aberdare Dolerite|69035|5|Briefly described|pp412-415 Fig.1, p429|||~ 600 to 700 m thick. Dips uniformly 30 to 45 degrees to the West. Previously interpreted as the closure of the Golden Mile Dolerite sill about the Kalgoorlie anticline (Campbell, 1953; Woodall, 1965; Travis, Woodall and Bartram, 1971).|||||Weakly differentiated gabbroic sill.|
21097|Aberdare Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 Ma (inferred).|Great Boulder Suite|||Weakly differentiated dolerite and gabbro; metamorphosed.|
21097|Aberdare Dolerite|70287|6|Mentioned|p188|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.||||||
21097|Aberdare 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.|||Weakly differentiated dolerite and gabbro; metamorphosed|
21097|Aberdare Dolerite|72095|5|Briefly described|p10-11, 14-17,20, 21|||Kalgoorlie Region, Eastern Goldfields, Yilgarn Craton. Detailed geochemistry is described.||||||
21097|Aberdare Dolerite|73300|6|Mentioned|p1113|||Yilgarn Craton, Kalgoorlie terrane.||||||
21103|Airfield Granodiorite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
21103|Airfield 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
21103|Airfield Granodiorite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
21103|Airfield Granodiorite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
21103|Airfield Granodiorite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
21103|Airfield Granodiorite|50437|5|Briefly described|p1.5, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
21103|Airfield Granodiorite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite.|||Medium- to coarse-grained, porphyritic biotite granodiorite and monzogranite.|30-JUL-15
21103|Airfield Granodiorite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Medium to coarse grained, porphyritic biotite granodiorite and monzogranite.|
21103|Airfield Granodiorite|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)||||Medium- to coarse-grained, porphyritic biotite granodiorite and monzogranite|
21103|Airfield Granodiorite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite||||
21103|Airfield Granodiorite|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 granodiorite and monzogranite|
21103|Airfield Granodiorite|72437|5|Briefly described|p80, p83|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated biotite-monzogranite and foliated porphyritic biotite granodiorite.|
21138|Angelo Microgranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c.1845Ma.||||||07-NOV-08
21138|Angelo Microgranite|23383|4|Described|p11, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex. Composed of altered, medium- to fine-grained, granophyric and granular microgranite.  Intrudes Koongie Park Formation.  Age: c.1845Ma. Geological Province: Hooper Orogen.  See also p6 Fig. 3.||||||07-NOV-08
21138|Angelo Microgranite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Altered medium- to fine-grained granophyric microgranite; disseminated malachite locally present.  Within the Lamboo Complex.||||||07-NOV-08
21138|Angelo Microgranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the San Sou Suite. Age: 1800Ma. Geological province: Kimberley Province .||||||07-FEB-11
21138|Angelo Microgranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Altered medium- to fine-grained granophyre; disseminated malachite locally. In the Lamboo Complex (Central zone).||||||07-NOV-08
21138|Angelo Microgranite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
21138|Angelo Microgranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Koongie Park Suite.||||||07-NOV-08
21138|Angelo Microgranite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Altered, medium- to fine-grained granophyre.||||||09-DEC-08
21138|Angelo Microgranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Of Koongie Park Formation?|||Medium- to fine-grained, granophyric to granular metamonzogranite; foliated; locally disseminated malachite.|30-JUL-15
21138|Angelo Microgranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.||Koongie Park Formation|||Medium- to fine-grained, granophyric to granular metamonzogranite; foliated; locally disseminated malachite.|
21138|Angelo 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; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1841-1841 Ma (Inferred)|Unit of Koongie Park Formation.|||Medium- to fine-grained, granophyric to granular metamonzogranite; foliated; locally disseminated malachite|
21138|Angelo Microgranite|70812|5|Briefly described|p13, p20|||||Koongie Park Formation|||Felsic porphyries.|
21138|Angelo 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 (183 -1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1841 Ma (inferred)|Unit of Koongie Park Formation.|||Medium- to fine-grained, granophyric to granular metamonzogranite; foliated; locally disseminated malachite|
21152|Arranoo Member|12758|5|Briefly described|p66 Tb. 9|||Of the Kockatea Shale.  Geological Province:  Allanooka High (Perth Basin).||||||20-OCT-04
21152|Arranoo Member|23279|5|Briefly described|p20-1|||||||||
21152|Arranoo Member|23520|5|Briefly described|p11 Fig. 7|Early Triassic|Early Triassic|Of the Kockatea Shale.   Geological Province: Perth Basin.||||||
21152|Arranoo Member|24443|5|Briefly described|Fig.30|Early Triassic|Early Triassic|Of Kockatea Shale. Geological Province: Bight Basin.||||||
21152|Arranoo Member|43495|5|Briefly described|9-32||Scythian|||||||
21152|Arranoo Member|60377|5|Briefly described|p61 Fig. 3|Scythian|Scythian|Of the Kockatea Shale. Geological Province: Perth Basin. Marine depositional environment.||||||07-FEB-11
21152|Arranoo Member|61546|6|Mentioned|p385 Fig.5.|Early Triassic|Early Triassic|||Unit in Kockatea Shale.||||
21152|Arranoo Member|61811|5|Briefly described|p21, p22, p62.|||Called Arranoo Sandstone Member on p62. Type section details in Appendix 1.||Unit in Kockatea Shale.||||
21152|Arranoo Member|67370|4|Described|p312, p334.|Early Triassic|Early Triassic|Renamed; formerly Arranoo Sandstone Member. It includes other lithologies than sandstone alone. Several prior references also omitted the lithology from the name. Dongara oil and gas field, Perth Basin. A minor oil and gas reservoir. Contains the K. saeptatus Oppel Zone.||Unit in upper Kockatea Shale.||Is overlain by Woodada Formation.|A finely-laminated sequence of interbedded fine-grained sandstone, siltstone and shale.|
21212|Bedout Volcanics|13255|6|Mentioned|p369|Late Permian|Late Permian|Roebuck Basin. Late Permian.||||||29-SEP-15
21212|Bedout Volcanics|69297|6|Mentioned|p337, p352|Changhsingian|Capitanian|Roebuck Basin.||||Overlain by the Locker Shale. Unconformably overlies the Liveringa Group.||
21212|Bedout Volcanics|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Wuchiapingian|Capitanian|Roebuck Basin.||||Overlies Liveringa Group. Is overlain by Locker Shale.||
21361|Bulla Rocks Monzogranite|24196|5|Briefly described|p45, p46, p70|Archean|Archean|Age: 2660 +/- 5 Ma (Black et al., 2002). Geological Province: South Murrin sub-domain, Yilgarn Craton.||||||07-NOV-08
21361|Bulla Rocks Monzogranite|24494|5|Briefly described|p38 App.1|||See also Bulla Rocks monzogranite||||||
21361|Bulla Rocks Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21361|Bulla Rocks Monzogranite|64633|5|Briefly described|p22.|Neoarchean|Neoarchean||2660 +/- 5 Ma.|||||
21361|Bulla Rocks Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Fine- to coarse-grained biotite monzogranite; K-feldspar phenocrysts, locally megacrystic; foliated.||||||07-FEB-11
21361|Bulla Rocks Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. OZCHRON1. Original comment: 'The age of 2660.3+-4.7 Ma is derived from the 10 oldest overgrowths, and is assigned to the crystallisation of this granite'.|2660+/-5 Ma U-Pb SHRIMP||||Fine- to coarse-grained biotite monzogranite; K-feldspar phenocrysts, locally megacrystic; foliated.|05-MAY-21
21361|Bulla Rocks Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also GA_geochron.csv and GA_rocks.csv|2660 +/- 5 (SHRIMP).||||Fine- to coarse-grained biotite monzogranite; K-feldspar phenocrysts, locally megacrystic; foliated.|
21361|Bulla Rocks Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
21361|Bulla 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 coarse-grained biotite monzogranite; K-feldspar phenocrysts, locally megacrystic; foliated|
21405|Butler Creek Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Rudall Complex, Paterson Orogen.||||||
21405|Butler Creek Formation|23590|6|Mentioned|p8|||||||||
21405|Butler Creek Formation|23602|4|Described|p11|||See also page 6 Table 1. Of Rudall Complex. Overlying unit Poynton Formation. Underlying unit Cassandra Member. Max. thickness: >1000 m.||||||
21405|Butler Creek Formation|23760|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Geological Province: Talbot Terrane.||||||07-NOV-08
21405|Butler Creek Formation|43848|5|Briefly described|Map Legend||Proterozoic|Rudall Complex.||||||
21405|Butler Creek Formation|50436|5|Briefly described|p2.1|||Overlies: Yandagooge Formation. Intruded by: Kalkan Supersuite.||||||
21405|Butler Creek Formation|64580|6|Mentioned|map legend|||Quartzite, psammitic paragneiss, banded paragneiss, and pelitic schist.||||||15-DEC-08
21405|Butler Creek Formation|64943|4|Described| p10, p11, p4-6, p8-9,19,20,28,38,39|Statherian|Statherian|Talbot Terrane, Rudall Complex. Banded paragneiss, schist, psammitic gneiss, BIF, quartzite. <1 km thick; thickens to the E and NE; type locality given. Underlies Poynton Formation conformably to disconformably. Age from 1787-1765 Ma intrusions.||||||
21405|Butler Creek Formation|65403|6|Mentioned|p11.|||The westward extension of a banded paragneiss which outcrops in the Connaughton Hills.||||||
21405|Butler Creek 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
21405|Butler Creek Formation|67202|5|Briefly described|p56|||Talbot Terrane, Rudall Complex. Over 1km thick. Minimum age from intruding granite.|>1790 Ma.||||Pelitic schist, paragneiss and local BIF.|
21405|Butler Creek Formation|68981|5|Briefly described|p3|||Eastern Talbot Terrane, Rudall Province.||||Overlies Yandagooge Formation.|Banded paragneiss; minor amphibole-chlorite schist.|
21405|Butler Creek Formation|71169|5|Briefly described|p3-p4, p6-p7, p14, p18, p60|||||||Structurally overlies the Yandagooge Formation. Structurally overlain by the Poynton Creek Formation.|Psammitic metasedimentary rocks, including quartz-feldspar-biotite gneiss, quartz-muscovite-feldspar schist, muscovitic quartzite, quartz-biotite schist and rare banded iron formation.|
21405|Butler Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, quartzite, mafic schist, gneiss|
21405|Butler Creek Formation|71795|6|Mentioned|p35 fig 4|||Rudall Province.||||||
21405|Butler Creek Formation|73168|6|Mentioned|p741 Fig.2|Mesoproterozoic|Paleoproterozoic|Rudall Province.||||||
21408|Cable Beach Sand|64449|2|Defined|p75, p76, p79 Tb. 5, p85-89|Holocene|Holocene|Includes Lombadina Conglomerate Member and Cape Boileau Member. Overlies Port Smith Sand, underlies Shoonta Hill Sand. Age: 1090+/-160 yrs BP, 2100 +/-180 yrs BP. Thick: 3m. Medium to fine to coarse sand and shelly sand (see p85-89).||||||07-FEB-11
21408|Cable Beach Sand|73213|5|Briefly described|955, 958 Fig.3, 959, 964|||Derived from the Mowanjum Sand.||||Overlies Mowanjum Sand and Port Smith Sand. Interfingers with Cape Gourdon Formation. Laterally abuts Eighty Mile Beach Coquina.|White quartz sand with carbonate grains; reworked and abraded by waves.|19-JAN-23
21411|Cadjebut Formation|22814|6|Mentioned|p250|||||||||
21411|Cadjebut Formation|23903|5|Briefly described|p1597 Fig.2|Givetian|Givetian|Geological Province: Canning Basin.||||||10-NOV-08
21411|Cadjebut Formation|63938|3|Fully described|p48-55|Givetian|Givetian|Vuggy dolomite, interbedded siltstone, evaporites and breccia. Incl. stromatolites and corals. Unconform. overlies Gap Creek Fm, Emanuel Formation. Transitional into Pillara Lst. May correlate with Dominic Shale. 30-60m thick. Hosts Zn-Pb mineralisation.||||||
21411|Cadjebut Formation|64159|5|Briefly described|p91 Fig. 6|Givetian|Givetian|Part of the Lennard Reef facies development.||||||
21411|Cadjebut Formation|64502|5|Briefly described|p765 Fig. 2, p768 Fig.5|Givetian|Givetian|||||||
21411|Cadjebut Formation|64580|4|Described|map legend||Givetian|Siltstone, shale, dolomite, evaporites (leached in outcrop), and sandstone. Givetian-Frasnian reef complexes, platform facies.||||||10-NOV-08
21411|Cadjebut Formation|64643|3|Fully described|p5 Fig. 4, p30, 31, App. p33-39|Givetian|Givetian|Vuggy dolomite, interbedded siltstone, evaporites and breccia. Incl. stromatolites and corals. Unconform. overlies Gap Creek Fm, Emanuel Formation. Transitional into Pillara Lst. May correlate with Dominic Shale. 30-60m thick. Hosts Zn-Pb mineralisation.||||||
21411|Cadjebut Formation|65214|6|Mentioned|p277|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
21411|Cadjebut Formation|65486|5|Briefly described|p6-7 Fig.5,6, p9 Fig. 7, Plate 1.|Givetian|Givetian|Dolomite, siltstone, shale, sandstone and evaporites, Canning Basin. Unconformably overlies Prices Creek Group. Underlies Gogo Formation, Sadler Limestone, Pillara Limestone.||||||
21411|Cadjebut Formation|66127|3|Fully described|pp19-26, p68, p204, Plates 4, 5, 7, 8.|Late Givetian|Late Givetian|Of Hocking et al. (1996); previously part of Pillara Limestone (Playford and Lowry, 1966). Named after Cadjebut Spring; type section on SW side of Emanuel Range c. 300 m north of Emanuel Creek. Bank subfacies: coastal shoal and hypersaline lagoon deposits. 52m thick in type section. Epigenetic Pb-Zn mineralization.||||Unconformably overlies Prices Creek Group and is conformably overlain by Pillara Limestone.|Vuggy unfossiliferous dolomite, interbedded siltstone, evaporites and breccia, leached in outcrop; relict stromatolites and coral common.|
21411|Cadjebut Formation|67131|6|Mentioned|p3 Fig. 2,|Givetian|Givetian|Bank subfacies.|||||Limestone.|
21411|Cadjebut Formation|69099|5|Briefly described|500k_geologyp08_lut.csv||Givetian|Givetian-Frasnian reef complexes, platform facies (reefal pre-cursor).||||Underlies Pillara Limestone.|Siltstone, shale, dolomite, evaporites (leached in outcrop), and sandstone.|30-JUL-15
21411|Cadjebut Formation|69165|4|Described|500k_geologyp08_lut.csv|Givetian|Givetian||||||Siltstone, Shale, Dolomite, evaporites and sandstone.|
21411|Cadjebut Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Givetian|Givetian||382-387 Ma||||Siltstone, shale, dolomite, evaporites (leached in outcrop), and sandstone|
21411|Cadjebut Formation|71267|5|Briefly described|500k_interpgeop16_lut.csv|Givetian|Givetian|Of Lennard Shelf, Canning Basin. Devonian reef complexes. 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).|387.7-382.7 Ma (inferred)||||Siltstone, shale, dolomite, evaporites (leached in outcrop), and sandstone|
21411|Cadjebut Formation|72034|5|Briefly described|500k_interpgeop16_lut|Givetian|Givetian|Reef complexes, platform facies, Lennard Shelf, Canning Basin.|||||Siltstone, shale, dolomite, evaporites (leached in outcrop), and sandstone.|
21411|Cadjebut Formation|72502|6|Mentioned|p5|Givetian|Givetian|Lennard Shelf, Canning Basin.||||Overlain by Gogo Formation, Sadler Limestone, and Pillara Limestone. Equivalent to Napier Formation.||
21433|Canning Gap Shale Member|64772|6|Mentioned|p41 Tb. 11|||Zone 2 of Hematite¿goethite zones of the Frere Formation.||||||25-NOV-13
21525|Como Sandstone Member|12759|4|Described|p43; p28 Tb. 7; p32 Fig 15; p36 Fig 17|Eocene|Paleocene|New name. Named from: Como suburb, S of Perth. Type Section: Bore AM40, between 326-383 m depth (max 57 m onshore) at AMG Zone 50 (394605m E, 6460132m N). Introduced in this study as the lowermost unit of the Kings Park Formation. Probably occupies a marine channel of limited extent. Forms a minor confined aquifer.||Unit of the Kings Park Formation.|||Predominantly medium-grained, moderately sorted, subangular to subrounded, pale grey to pale greenish-grey, slightly clayey sand.|12-MAY-14
21525|Como Sandstone Member|68254|6|Mentioned|p1039, p1040 Tb.3|||Member status specified in column heading of Table 3. See informal Como Sandstone in this paper. Described as minor aquifer.||Of the Kings Park Formation.|||Sandstone.|20-JUL-15
21525|Como Sandstone Member|68811|6|Mentioned|p180 tbl 39|Tertiary|Tertiary|||Of Kings Park Formation.||||15-APR-20
21659|Dillinger Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs suite.||||||07-NOV-08
21659|Dillinger Monzogranite|23383|4|Described|p14, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Sally Downs supersuite (Lamboo Complex). Composed of medium-grained, even textured or weakly porphyritic, leucocratic biotite monzogranite, and minor syenogranite. Intrudes Emull Gabbro. Age: 1820-1805Ma.  Geol.Prov:  Halls Creek Orogen.||||||07-NOV-08
21659|Dillinger Monzogranite|23599|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Age: 1820-1805 Ma. Of Sally Downs supersuite.||||||07-NOV-08
21659|Dillinger Monzogranite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Medium- to fine-grained, locally porphyritic, leucocratic biotite monzogranite, minor syenogranite; abundant mafic inclusions adjacent to contacts with gabbro.||||||07-NOV-08
21659|Dillinger 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
21659|Dillinger Monzogranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite. Medium- to fine-grained, porphyritic leucocratic biotite monzogranite; minor syenogranite; rich in mafic inclusions adjacent to contacts with gabbro. Age: 1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
21659|Dillinger Monzogranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
21659|Dillinger Monzogranite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
21659|Dillinger 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
21659|Dillinger Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|||Medium- to fine-grained, leucocratic biotite monzogranite; minor syenogranite; rich in mafic inclusions adjacent to contacts with gabbro.|30-JUL-15
21659|Dillinger Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite||Intrudes into Emull Gabbro|Medium-fine grained, leucocratic biotite monzogranite; minor syenogranite; rich in mafic inclusions adjacent to contacts with gabbro.|
21659|Dillinger 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 fine-grained, leucocratic biotite monzogranite; minor syenogranite; rich in mafic inclusions adjacent to contacts with gabbro|
21659|Dillinger Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Medium- to fine-grained, leucocratic biotite monzogranite; minor syenogranite; rich in mafic inclusions adjacent to contacts with gabbro|
21659|Dillinger 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 fine grained, locally porphyritic leucocratic biotite monzogranite and minor syenogranite; rich in mafic inclusions adjacent to gabbro|
21659|Dillinger Monzogranite|72437|5|Briefly described|p102-103|||Whole rock analyses are provided.||Kevins Dam Suite|||Fine-grained biotite monzogranite, biotite monzogranite.|
21728|Eastman Granite|22754|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of San Sou suite. Age: c. 1805 Ma||||||07-NOV-08
21728|Eastman Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the San Sou Suite. Age: 1800Ma. Geological province: Kimberley Province .||||||07-FEB-11
21728|Eastman Granite|50437|5|Briefly described|p1.6, 5.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the San Sou Suite. Age: 1805 +/- 5Ma (SHRIMP).||||||21-MAY-21
21728|Eastman Granite|63866|5|Briefly described|p129-p130, p132, p138|Orosirian|Orosirian|Eastern Zone, Halls Creek Orogen. Appears as the Eastmans Granite on p130 and p138.|c. 1804 Ma|Sally Downs Supersuite||||
21728|Eastman Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Fine to coarse grained biotite syenogranite and monzogranite.||||||09-DEC-08
21728|Eastman Granite|66845|4|Described|p537 Fig.3, p539 Tb.1, p543, p544 Fig.10|||One zircon core had 207Pb/206Pb age of 1862+/-6 Ma.|18 analyses, magmatic age 1804+/-5 Ma SHRIMP U-Pb|San Sou suite|||Coarse biotite monzogranite.|31-JUL-15
21728|Eastman Granite|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|Described with San Sou Monzogranite.|||||Fine- to coarse-grained biotite syenogranite and monzogranite.|
21728|Eastman Granite|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Is this name still in use? Grouped with San Sou Monzogranite in 500k_geologyp08_lut.csv. Lith description is for both units.|||||Fine to coarse grained biotite syenogranite and monzogranite|31-JUL-15
21728|Eastman Granite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Fine to course grained biotite syenogranite and monzogranite|
21728|Eastman Granite|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Fine to course grained biotite syenogranite and monzogranite|
21728|Eastman Granite|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1804 Ma||||Medium- to coarse-grained, leucocratic biotite syenogranite and monzogranite|
21728|Eastman Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|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, 2_5m_interpgeop15_lut.csv.|1804+\-5 Ma (isotopic)||||Fine to coarse grained leucocratic biotite syenogranite, monzogranite and monzonite|
21728|Eastman Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|1804+/-5 Ma.||||Medium- to coarse-grained, leucocratic biotite syenogranite and monzogranite.|
21728|Eastman Granite|72437|6|Mentioned|p11, p110|Palaeoproterozoic|Palaeoproterozoic|||San Sou suite||||
21728|Eastman Granite|73089|6|Mentioned|p40-41|Statherian|Orosirian|Halls Creek Orogen, southern.|1804 +/- 5 Ma|||||
21735|Eighty Mile Beach Coquina|64449|2|Defined|p75, p79 Tb. 5, p83-85|Holocene|Holocene|Overlies: Port Smith Sand (sharp contact). Underlies; Shoonta Hill Sand (sharp contact). Age: 3680+/-210 yrs BP. Thickness: 3m. Consists of shell gravel; ribbon deposit mainly formed under a winnowed beach face. See p 83-85 for detailed information.||||||07-FEB-11
21735|Eighty Mile Beach Coquina|73213|6|Mentioned|958 Fig.3(b)|||||||Overlies Port Smith Sand. Laterally abuts Cable Beach Sand.||19-JAN-23
21754|Esaw Monzogranite|22754|5|Briefly described|p6, p8|||Of the Sophie Downs suite.  Age: c. 1910Ma.||||||
21754|Esaw Monzogranite|23599|4|Described|p8|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
21754|Esaw Monzogranite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
21754|Esaw Monzogranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Partly recrystallised, garnet-muscovite granite. Age: c.1910Ma.  In the Lamboo Complex (eastern zone).||||||07-NOV-08
21754|Esaw Monzogranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
21754|Esaw Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Sophie Downs Suite.||||||07-NOV-08
21754|Esaw Monzogranite|63866|5|Briefly described|p128-p129, p138|||Eastern Zone, Halls Creek Orogen.||||||
21754|Esaw Monzogranite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite.||||||09-DEC-08
21754|Esaw Monzogranite|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|Described with Junda Microgranite.|||||Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite.|
21754|Esaw Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Sophie Downs Suite|||Leucocratic biotite-muscovite metamonzogranite and garnet-muscovite metamonzogranite.|31-JUL-15
21754|Esaw Monzogranite|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Partly recrystallized; leucocratic monzogranite and garnet muscovite granite.|
21754|Esaw Monzogranite|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Partly recrystallized; leucocratic monzogranite and garnet-muscovite granite|
21754|Esaw Monzogranite|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.|1913-1907 Ma (Inferred)|Unit of Sophie Downs Suite.|||Leucocratic biotite-muscovite metamonzogranite and garnet-muscovite metamonzogranite|
21754|Esaw Monzogranite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1907-1913 Ma||||Leucocratic biotite-muscovite metamonzogranite and garnet-muscovite metamonzogranite.|
21754|Esaw Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Coeval with Ding Dong Downs Volcanics. 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.|1912-1909 Ma (inferred)|Unit of Sophie Downs Suite.|||Leucocratic biotite-muscovite metamonzogranite and garnet-muscovite metamonzogranite|
21754|Esaw Monzogranite|71397|5|Briefly described|p8,10|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen.||Unit of Sophie Downs Suite.|||Leucocratic biotite-muscovite monzogranite and garnet-muscovite monzogranite.|
21754|Esaw Monzogranite|72437|5|Briefly described|p7, p51|Palaeoproterozoic|Palaeoproterozoic|Analysed (three times) in this study.|c. 1910 Ma|Sophie Downs suite|||Biotite-muscovite monzogranite, garnet-mica leucogranite.|
21760|Eureka Dolerite|23926|6|Mentioned|p19 Fig. 7|||||||||
21760|Eureka Dolerite|42969|6|Mentioned|p106|||||||||
21760|Eureka Dolerite|63163|5|Briefly described|p76|||A sill with maximum thickness: 200m. Similar in composition to, and spatially associated with, the high Fe tholeiitic portion of Paringa Basalt. Geological Province: Kalgoorlie Terrane/Eastern Goldfields Province.||||||07-FEB-08
21760|Eureka Dolerite|65834|6|Mentioned|p53-54, 56|||Kalgoorlie Goldfield. Initially thought to be extension of Golden Mile Dolerite.||||||
21760|Eureka Dolerite|69035|5|Briefly described|p412, p413 Colour Plate 1, p414 Tb.3|||~ 50 to 220 m thick. Previously interpreted as stratigraphically thinned Golden Mile Dolerite on the east limb of the Kalgoorlie anticline. Located at or near the top of the magnesian part of the Paringa Basalt.|||||Weakly differentiated gabbroic sill.|02-JUL-14
21760|Eureka Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Weakly differentiated dolerite sill; minor granophyric zone; ophitic textures; subordinate quartz; metamorphosed.|
21760|Eureka Dolerite|70287|6|Mentioned|p188|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.||||||
21760|Eureka 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.|||Weakly differentiated dolerite sill; minor granophyric zone; ophitic textures; subordinate quartz; metamorphosed|
21760|Eureka Dolerite|72095|4|Described|p10-11, 14-17,20, 21|||Kalgoorlie Region, Eastern Goldfields, Yilgarn Craton. Detailed geochemistry is described.||||Similar stratigraphic level as Golden Mile Dolerite. Volcanic equivalent probably underlies Black Flag Group in SE18W1.|Dolerite sill.|10-MAY-23
21760|Eureka Dolerite|73300|6|Mentioned|p1112-1113|||Yilgarn Craton, Kalgoorlie terrane.|||||Dolerite sill, intrudes volcano-sedimentary sequence.|
21760|Eureka Dolerite|73391|6|Mentioned|Appendices.|||Clout et al. (1990). Regional stratigraphic correlation chart of other workers.|||||Weakly differentiated gabbro sill.|
21775|Federal Dolerite|23926|6|Mentioned|p19 Fig. 7|||||||||
21775|Federal Dolerite|62108|5|Briefly described|p1420 Fig. 14|||In the Kalgoorlie district. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
21775|Federal Dolerite|65834|6|Mentioned|p54, 56|||Kalgoorlie district.||||||
21775|Federal Dolerite|69035|5|Briefly described|p412, p413 Cp.1, p414 Tb.3, p415 Fig.1|||~ 85 to 100 m thick differentiated sill.|||||Weakly differentiated gabbroic sill.|
21775|Federal Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Weakly differentiated dolerite sill; minor granophyric zone; ophitic textures; subordinate quartz; metamorphosed.|
21775|Federal Dolerite|70287|6|Mentioned|p188|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.||||||
21775|Federal 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.|||Weakly differentiated dolerite sill; minor granophyric zone; ophitic textures; subordinate quartz; metamorphosed|
21775|Federal Dolerite|73300|6|Mentioned|p1112-1113|||Yilgarn Craton, Kalgoorlie terrane.|||||Dolerite sill, intrudes volcano-sedimentary sequence.|
21775|Federal Dolerite|73391|6|Mentioned|Appendices.|||Clout et al. (1990). Regional stratigraphic correlation chart of other workers.|||||Differentiated gabbroic sill.|
21787|Fingoon Quartzite|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Rudall Complex, Paterson Orogen.||||||
21787|Fingoon Quartzite|23602|4|Described|p9|||See also page 6 Table 1. Of Rudall Complex. Overlying unit Yandagooge Formation. Underlying unit Larry Formation. Max. thickness: 1500 m.||||||
21787|Fingoon Quartzite|23760|4|Described|p14|Statherian|Statherian|Age: c.1790 Ma. Geological Province: Talbot Terrane. Max. thickness: 1500 m.||||||
21787|Fingoon Quartzite|43348|6|Mentioned|P5|||Of Rudall Complex?||||||
21787|Fingoon Quartzite|43848|5|Briefly described|Map Legend||Proterozoic|||||||
21787|Fingoon Quartzite|50436|5|Briefly described|p2.1|||Conformably overlies: Larry Creek Formation. Conformably underlies: Yandagooge Formation.||||||
21787|Fingoon Quartzite|63866|5|Briefly described|p141, p143|Statherian|Orosirian|Talbot Terrane, Rudall Complex. Numeric age range is derived from U-Pb zircon geochronology.|1800-1790 Ma (Nelson, 1995)|||||
21787|Fingoon Quartzite|64580|6|Mentioned|map legend|||Quartzite, psammitic paragneiss, banded paragneiss, and pelitic schist.||||||15-DEC-08
21787|Fingoon Quartzite|64943|4|Described|p4-6, p8, 9,10,11,15-16,19,20,35-36,38|Statherian|Statherian|Of Talbot Terrane, Rudall Complex. Max thickness 1500m; dominantly massive or layered quartzite. Younger than 1790+/-10 Ma (Nelson 1995), based on clastic zircons. Type locality given. Conformably overlain by Yandagooge Formation.||||||
21787|Fingoon Quartzite|65403|6|Mentioned|p29 Table 3.|||Talbot Terrane.||||||
21787|Fingoon Quartzite|65454|5|Briefly described|p4-5|Statherian|Statherian|Of Fingoon Package, Talbot Terrane. Unimodal detrital zircon age of 1800-1790 Ma, consistent with derivation from the oldest felsic rocks in the region.||||||21-APR-16
21787|Fingoon Quartzite|67202|5|Briefly described|p56, p161|||Talbot Terrane, Rudall Complex. Over 1500m thick. Maximum depositional age from detrital zircons.|<1790 Ma (Nelson, 1995).|Rudall Complex.|||Quartzite and micaceous quartzite.|
21787|Fingoon Quartzite|68981|5|Briefly described|p2-4, p18|||Eastern Talbot Terrane, Rudall Province. Detrital zircon age (Nelson, 1995).|1791 +/- 10 Ma (maximum depositional age).|||Conformably overlies Larry Formation. Is overlain conformably by Yandagooge Formation.|A succession of quartzite and minor mica schist.|
21787|Fingoon Quartzite|69003|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Talbot Terrane, Paterson Orogen. Detrital zircon maximum depositional age.|<c.1790 Ma.|||||
21787|Fingoon Quartzite|71169|5|Briefly described|v, p1, p3-p6, p14, p18|Statherian|Statherian|Talbot Terrane, Rudall Province. A maximum depositional age of 1794 +/- 4Ma obtained from this study. Interpreted to have been sourced from exhumed granitic rocks of the Kalkan Supersuite. See also p24-p27, p59-p60, p65, p70, p87.|1791 +/- 10 Ma (Kirkland et al. 2013)|||Structurally overlies the Larry Formation. Structurally overlain by the Yandagooge Formation.|Muscovitic quartzite.|
21787|Fingoon Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, psammite, quartzite|
21787|Fingoon Quartzite|71795|5|Briefly described|p35 fig 4|||Rudall Province.||||||
21787|Fingoon Quartzite|73168|6|Mentioned|p741 Fig.2, p742|Mesoproterozoic|Paleoproterozoic|Rudall Province. Talbot Domain, eastern. Deposited after 1794-1791 Ma. Interpreted to represent a syn- or post-magmatic cover sequence derived from the Kalkan Supersuite.||||||
21803|Fly Flat Member|73344|2|Defined|p. 1, 3-6, 8-10, 12-15, 17-19, 31-32...|Tremadocian|Tremadocian|Canning Basin, central-western. Proposed new lower subdivision of the Nambeet Formation [article includes definition card]. Type section is from the Olympic 1 well between 1383.57 and 1447.53 m = 63.96 m thickness [also written as 63.53], although an additional ca 20 m of the unit below TD was inferred. Thickness varies between ~42 m to ~200 m. Top of the sandstone marks the top contact; probably disconformable. Interpreted to directly overlie basement. Named for the Fly Flat Bore ~21.3 km NNW of Olympic 1. Previously the informal 'lower sandstone unit' and 'basal transgressive deposits' of the Nambeet Formation. Known only from the subsurface. Described using three siliciclastic facies associations from eight facies [article includes detailed lithologic description]. Reflects open marine, upper-lower shoreface depositional environments; lowstand deposits. Part of supersequence A0. Covers part of the P. proteus conodont biozone at the type section and the P. elegans - Berg. extensus and Drepanastodus-Paltodus biozones in other wells. Other marine microfossils and bioturbation observed. Further divided into an upper fine-grained section and, in some places (not Olympic 1), an underlying basal sandstone-conglomerate unit (northwest Canning Basin). Basal coarse-clastic deposits inferred as equivalent to Kunian Sandstone. Low measured core porosity and permeability in Olympic 1 due to diagenetic quartz and carbonate cements, although the uppermost facies association may have reservoir potential. Contains a ca 30 cm thick residual oil show. Age constraint from biostratigraphy and radiometric ages in the overlying Samphire Marsh Member. More locations: p. 36-41, 43-44, 47, 50-53, 55-56, 62-65, Pl.1-2.||Nambeet Formation||Overlain by Samphire Marsh Member. Equivalent to Wilson Cliffs Sandstone and Emanuel Formation[?], Kudata Dolomite, and Kunian Sandstone of the Prices Creek Group.|Well-sorted, very fine- to fine-grained subarkose sandstone and minor siltstone; basal sandstone-conglomerate unit of variable character; common glauconite and traces of pyrite.|
21803|Fly Flat Member|73345|4|Described|p226-230|Tremadocian|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. Unit is nearly three times thicker in Barnicarndy 1 (173 m) than the type section in Olympic 1. Low permeability and porosity.||Nambeet Formation||Conformably underlain by Yapukarninjarra Formation. Conformably overlain by Samphire Marsh Member. Equivalent to Wilson Cliffs Sandstone.|Includes white, very-fine- to fine-grained sandstone with both siliceous and carbonate cements with siltstones and mudstones containing common glauconite and trace pyrite.|
21829|Galvalley Monzogranite|43148|5|Briefly described|map legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|43205|5|Briefly described|map legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|43207|5|Briefly described|map legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|43221|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|43293|3|Fully described|Appendix p18,p12.||Archean|age is interpreted as Post-D2 to syn-D3.||||||07-NOV-08
21829|Galvalley Monzogranite|43497|4|Described|5-18||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|43593|4|Described|Fig.3,p6,15|||||||||
21829|Galvalley Monzogranite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|44203|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21829|Galvalley Monzogranite|60076|5|Briefly described|p23, p45 App. 1|Archean|Archean|[Agmga]   K-feldspar-phyric biotite monzogranite; aligned K-feldspar, biotite, and xenoliths define foliation locally.||||||07-NOV-08
21829|Galvalley Monzogranite|64775|6|Mentioned|p3-1, 9-1|||Age: younger than Yarri Monzogranite||||||
21829|Galvalley Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Biotite monzogranite with prominent K-feldspar megacrysts; aligned K-feldspar, biotite, and xenoltihs define foliation locally.||||||07-FEB-11
21829|Galvalley Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite monzogranite with prominent K-feldspar megacrysts; aligned K-feldspar, biotite, and xenoliths define foliation locally.|06-AUG-15
21829|Galvalley Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite monzogranite with prominent K-feldspar megacrysts; aligned K-feldspar, biotite, and xenoliths define foliation locally.|
21829|Galvalley Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
21829|Galvalley 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 with prominent K-feldspar megacrysts; aligned K-feldspar, biotite, and xenoliths define foliation locally|
21871|Gnangara Sand|12759|1|Redefined|p43-7; p28 Tb. 7; p32 Fig 15; 36 Fig 17|Quaternary|Neogene|Informal - Morgan (1964b). Derived from Lake Gnangara N of Perth. Type section in Mirrabooka bore M270 at 21.5-46.5 m, (AMG Z50, 401222 m E, 6479624 m N). Max thickness 30 m.||Of Kwinana Group.||Unconformable on Kings Park, Ascot Formations. Interfingers with Guildford Clay. Overlain by Bassendean Sand (conformably) and Tamala Limestone (unconformably).|Pale grey, fine- to very coarse-grained, very poorly sorted (locally bimodal), subrounded to rounded quartz sand and abundant feldspar; predominantly fluvial.|15-APR-20
21871|Gnangara Sand|63745|5|Briefly described|p59|Middle Pleistocene||Stratigraphic equivalent of Guildford Formation, interfingering to the east with, and grading into, the Guildford Fm. Named Guildford Fm sand member by Deeney (1989). Conformable below Bassendean Sand. Sandy fluvial and estuarine sediments.||||||07-FEB-11
21871|Gnangara Sand|68811|5|Briefly described|p90|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
21872|Gnewing Granodiorite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
21872|Gnewing Granodiorite|23383|5|Briefly described|p8|||See also Gnewing granodiorite (p5 Tb. 1).  Of Paperbark supersuite. Hooper Orogen Province.||||||25-JAN-05
21872|Gnewing Granodiorite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Coarsely porphyritic, biotite-hornblende granodiorite and tonalite; contains mafic inclusions.  Part of the Bow batholith.||||||07-NOV-08
21872|Gnewing 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
21872|Gnewing Granodiorite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite. Coarsely porphyritic biotite-hornblende granodiorite and tonalite; contains mafic inclusions. Age: 1865-1850Ma.||||||07-NOV-08
21872|Gnewing Granodiorite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
21872|Gnewing Granodiorite|50437|5|Briefly described|p1.5, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
21872|Gnewing Granodiorite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Porphyritic biotite-hornblende granodiorite and tonalite; contains mafic inclusions.|31-JUL-15
21872|Gnewing Granodiorite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Porphyritic biotite--hornblende granodiorite and tonalite; contains mafic inclusions.|
21872|Gnewing Granodiorite|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.|||Porphyritic biotite-hornblende granodiorite and tonalite; contains mafic inclusions|
21872|Gnewing Granodiorite|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1852-1864 Ma|Paperbark Supersuite||||
21872|Gnewing Granodiorite|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.|||Porphyritic biotite-hornblende granodiorite and tonalite; contains mafic inclusions|
21872|Gnewing Granodiorite|72437|5|Briefly described|p79|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite-hornblende granodiorite.|
21913|Grimpy Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
21913|Grimpy Monzogranite|23383|4|Described|p14, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Sally Downs supersuite (Lamboo Complex).  Medium- to fine-grained, even textured or weakly porphyritic biotite granodiorite and tonalite, with lesser biotite monzogranite.  Geol. Prov: Halls Creek Orogen.||||||07-NOV-08
21913|Grimpy Monzogranite|23599|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Age: 1820-1805 Ma. Of Sally Downs supersuite.||||||07-NOV-08
21913|Grimpy Monzogranite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Weakly porphyritic, fine-grained biotite monzogranite.||||||07-NOV-08
21913|Grimpy 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
21913|Grimpy Monzogranite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Weakly porphyritic fine-grained biotite monzogranite.  Age: 1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
21913|Grimpy Monzogranite|44693|5|Briefly described|Map Legend||Proterozoic|||||||
21913|Grimpy Monzogranite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
21913|Grimpy Monzogranite|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
21913|Grimpy Monzogranite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Syenite Camp Suite|||Weakly porphyritic, fine-grained monzogranite.|31-JUL-15
21913|Grimpy Monzogranite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Syenite Camp Suite|||Weakly porphyritic, fine grained monzogranite.|
21913|Grimpy 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.|1817-1817 Ma (Inferred)|Unit of Syenite Camp Suite.|||Weakly porphyritic, fine-grained monzogranite|
21913|Grimpy Monzogranite|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1817 Ma|Syenite Camp Suite|||Weakly porphyritic, fine grained monzogranite|
21913|Grimpy 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). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1816 Ma (inferred)|Unit of Syenite Camp Suite.|||Medium- to fine-grained, even textured or weakly porphyritic biotite granodiorite and tonalite, with lesser biotite monzogranite.|
21913|Grimpy Monzogranite|72437|5|Briefly described|p99-100|||Whole rock analyses are provided.||Syenite Camp Suite|||Foliated granodiorite, biotite monzogranite, syenogranite.|
21919|Gunanya Sandstone|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
21919|Gunanya Sandstone|23602|4|Described|p16|||Of Tarcunyah Group. Overlying unit is Waters Formation. Max. thickness: 500 m.||||||23-MAY-16
21919|Gunanya Sandstone|23742|4|Described|p6|Mesoproterozoic|Mesoproterozoic|Of Tarcunyah Group. Geological Province: Paterson Orogen.||||||
21919|Gunanya Sandstone|23760|4|Described|p26|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
21919|Gunanya Sandstone|43848|5|Briefly described|Map Legend||Proterozoic|Tarcunyah Group.||||||
21919|Gunanya Sandstone|43849|5|Briefly described|Map Legend||Proterozoic|Age approx 800 Ma.||||||
21919|Gunanya Sandstone|43856|5|Briefly described|Map Legend||Proterozoic|||||||
21919|Gunanya Sandstone|50008|4|Described|p44|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group (in lower part). Fluvial to deltaic medium to coarse grained arkosic sandstone, with a source to the west and southwest. Thickness: 500m. Zircons used for dating and provenance studies. Geological Province: Officer Basin.||||||
21919|Gunanya Sandstone|60470|6|Mentioned|p2, p4 Fig. 2, p8|Neoproterozoic|Neoproterozoic|in Officer Basin, base of Tarcunyah Group. Includes detrital zircon populations giving 1070 Ma as max possible age for this unit. Sandstone; minor conglomerate, siltstone, and shale. Shown as lateral equivalent to Karara Formation.||||||
21919|Gunanya Sandstone|62453|4|Described|p5 Fig. 3, 64|Cryogenian|Tonian|Geological Province: Paterson Orogen. Of the Tarcunyah Group. Unconformably overlies: Rudall Complex. Sandstone, conglomerate. Thickness: ~500m.||||||
21919|Gunanya Sandstone|62986|5|Briefly described|p18|||At base of Tarcunyah Group. Geological Province: Yeneena Basin.||||||
21919|Gunanya Sandstone|64777|4|Described|p3 Fig.4, p4-8|Neoproterozoic|Neoproterozoic|500 m thick fluvial-deltaic succession. 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).|Unit in Tarcunyah Group.|||Sandstone; minor conglomerate, siltstone and shale. Medium-to coarse-grained arkosic sandstone; interbeds of coarse-grained, pebbly feldspathic sandstone are common in the top 100m.|
21919|Gunanya Sandstone|64943|5|Briefly described|p29, 30, 37|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Paleocurrent data supports sediment transport from SW.||||||
21919|Gunanya Sandstone|65403|4|Described|pp13-14, p20, p28.|||Has lithological, stratigraphic and structural similarities with Karara Formation. Probable equivalent to Choorun (and Nooloo) Formations. Abundant ripples and cross-beds indicate a SW-directed current in a fluvial to deltaic environment.||Unit in Tarcunyah Group.||Disconformably overlies Pungkuli Formation. Is conformably overlain by Waters Formation.|Medium- to coarse-grained, light-pink to purple, arkosic sandstone interbedded with thin pebbly horizons and beds of feldspathic grit.|
21919|Gunanya Sandstone|65454|5|Briefly described|p10-11|Cryogenian|Cryogenian|Of Throssell Range Group and correlated with Coolbro Sandstone (Czarnota et al. 2009). Formerly assigned to Tarcunyah Group (Grey et al. 2005).||||||
21919|Gunanya Sandstone|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Officer Basin. Shown as lateral equivalent of  Karara Formation.||||||23-MAY-16
21919|Gunanya Sandstone|67202|4|Described|p64-65, p231|Neoproterozoic|Neoproterozoic|NW Officer Basin. Also appears as Gunanyah Sandstone (p65). Detrital zircon maximum (text says minimum) depositional age.|< c.950 Ma (Bagas and Nelson, 2007).|Tarcunyah Group.||Is overlain by Waters Formation. Correlated with Coolbro Sandstone.|Conglomerate, arkose, coarse- to medium-grained sandstone, siltstone.|
21919|Gunanya Sandstone|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
21955|Henley Sandstone Member|12759|2|Defined|p38-9; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Albian|Late Aptian|Named from Henley Brook, NE of Perth. Type Section: Bore AM11, at AMG Zone 50 (406475 m E, 6524957 m N) 229-270 m depth (max 100 m).||Base of Osborne Fm.||Unconformably overlies Wanneroo and Pinjar Members; overlain conformably by Kardinya Shale Member.|Sandstone, dark greenish-brown and glauconitic; minor siltstone.|12-MAY-14
21955|Henley Sandstone Member|14227|5|Briefly described|Enclos. 2|Early Cretaceous|Early Cretaceous|Of Coolyena Group. Probably of Osborne Formation. Presented as Henley Sst Mem.||||||07-FEB-11
21955|Henley Sandstone Member|23279|6|Mentioned|p31|||||||||
21955|Henley Sandstone Member|68254|6|Mentioned|p1040 Tb.3, p1046 Tb.4|||Member status specified in column heading of Table 3. See informal Henley Sandstone in this paper.||Of the Osborne Formation.||||
21955|Henley Sandstone Member|68811|6|Mentioned|p180 tbl 39|Cretaceous|Cretaceous|Part of Leederville aquifer.||Of Leederville Formation?||||15-APR-20
21955|Henley Sandstone Member|70099|5|Briefly described|p6|||Southern Perth Basin. Correlated to Mentelle 8 Supersequence of mainly deep marine ferruginous mudstones.||Osborne Formation.|||Includes glauconitic sandstones and siltstones.|
21963|Hill River Coal Measures|43297|6|Mentioned|Fig.5 p9.|||of Cattamarra Group. Informal name.||||||
10003|Lady Mary Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
10003|Lady Mary Member|43162|6|Mentioned|6|||||||||
10004|Lady Miller Jaspilite Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
10004|Lady Miller Jaspilite Member|43162|6|Mentioned|6|||||||||
10051|Lake George Formation|41751|6|Mentioned|p8|||||||||
10051|Lake George Formation|43818|6|Mentioned|Fig.2.p39||Cenozoic|||||||19-NOV-08
10051|Lake George Formation|44143|4|Described|p430 Table 4-19; p.452 Fig. 4-113|Eocene|Eocene|Up to 5 m thick; sandstone and conglomerate; fluvial. Unconformably overlies Anketell Sandstone and Callawa Formation. Type section 8 km SE of Helen Hill (TABLE TOP: 22deg 50'00" S, 123deg 42'55" E).||||||10-FEB-20
10051|Lake George Formation|65301|5|Briefly described|p5 Fig. 4|||Geological province: Canning Basin.||||||
10051|Lake George Formation|65449|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|||||||
10051|Lake George Formation|68007|6|Mentioned|p4|Late Cretaceous|Late Cretaceous|Canning Basin.||||||25-FEB-20
10051|Lake George Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||||
10051|Lake George Formation|70774|5|Briefly described|p4|Late Cretaceous|Late Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||||10-FEB-20
10051|Lake George Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
10051|Lake George Formation|73117|5|Briefly described|p3|Upper Cretaceous|Upper Cretaceous|Canning Basin.||||Equivalent[?] to Lampe Formation.|Dominantly sandstone with lesser shale.|
10055|Lake Gregory beds|7433|5|Briefly described|p48 Fig.43, p50. |Tertiary|Late Cretaceous|Canning Basin. At least 99 m thick. Grainsize increases in upstream palaeochannels of Sturt Creek. Evaporites occur where water table is close to surface.|||||Red, green and buff-coloured fine clastics, grading into coarser clastics and minor calcrete; pebbles of laterite pisoliths; calcrete and powdery caliche common adjacent to and within playas. Rare gypsum, halite.|
10055|Lake Gregory beds|38878|6|Mentioned|Map legend|Pliocene|Miocene|Miocene - Pleistocene||||||
10055|Lake Gregory beds|45153|2|Defined|App.11-170|late Tertiary|late Tertiary|||||||
10055|Lake Gregory beds|45158|3|Fully described|p10|||See also P34||||||
10055|Lake Gregory beds|61155|5|Briefly described|p16|Holocene|Late Pliocene|Age: <3Ma. Thickness: 99m. Geological Province: Fitzroy Graben.||||||
10055|Lake Gregory beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||silcrete, lacustrine sediment|
10057|Lake Johnston Granite|36566|6|Mentioned|Fig.1|||||||||
10059|Lake Kwornicup gneiss|38578|6|Mentioned|p14|||||||||
10070|Lake Shaster Monzonite|40811|4|Described|p320|||||||||
10070|Lake Shaster Monzonite|43715|6|Mentioned|p28|||||||||
10094|Lally Conglomerate|22754|5|Briefly described|p5 Tb. 1|Cambrian|Neoproterozoic|||||||
10094|Lally Conglomerate|23383|5|Briefly described|p22, p5 Tb. 1||Cambrian|Massive, cross-bedded medium- to coarse-grained sandstone, with local lenses of quartz cobble conglomerate. Conformably overlain by Antrim Plateau Volcanics. Max thickness: <33 m.  Geological Province: Ord Basin/King Leopard Orogen.  See also p6 Fig. 3.||||||25-JAN-05
10094|Lally Conglomerate|23599|4|Described|p19|Cambrian|Cambrian|Age: c.540 Ma. Overlying unit Antrim Plateau Volcanics. Geological Province: Ord Basin. Max. thickness: 33 m.||||||
10094|Lally Conglomerate|23601|5|Briefly described|Map legend|Cambrian|Cambrian|Medium- to coarse-grained quartz sandstone, and cobble conglomerate.  Geological Province: Ord Basin.||||||25-JAN-05
10094|Lally Conglomerate|24503|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Ord and Bonaparte Basins.||||||
10094|Lally Conglomerate|30895|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10094|Lally Conglomerate|32728|6|Mentioned|Fig.3|||||||||
10094|Lally Conglomerate|36898|6|Mentioned|p183|||||||||
10094|Lally Conglomerate|37927|6|Mentioned|p506|||||||||
10094|Lally Conglomerate|43281|6|Mentioned|Map legend||Cambrian|||||||
10094|Lally Conglomerate|44231|5|Briefly described|Map Legend|Cambrian|Cambrian|Fine- to coarse-grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone, and quartz sandstone. Geological Province: Ord Basin.||||||19-MAY-05
10094|Lally Conglomerate|44397|14|Not recorded|p.10,15,20,Table 4|||L.Camb.(?). Defn. on Tech.File E/52-9.||||||
10094|Lally Conglomerate|44398|14|Not recorded|map legend|||Lower Cambrian (?)||||||
10094|Lally Conglomerate|44693|5|Briefly described|Map Legend||Cambrian|||||||
10094|Lally Conglomerate|44694|5|Briefly described|Map Legend||Cambrian|||||||
10094|Lally Conglomerate|48927|2|Defined|p33|Adelaidean|Adelaidean|||||||
10094|Lally Conglomerate|63458|6|Mentioned|p897 Fig.19. |Cambrian|Cambrian|||||||
10094|Lally Conglomerate|64580|4|Described|map legend|Middle Cambrian|Middle Cambrian|Conglomerate.||||||09-DEC-08
10094|Lally Conglomerate|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut.csv|Middle Cambrian|Middle Cambrian|||||Is overlain by Antrim Plateau Volcanics.||
10094|Lally Conglomerate|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Stage 5|Ord Basin. Grouped as Antrim Plateau Volcanics and Lally Conglomerate.|||||Fine- to coarse-grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone and quartz sandstone.|31-JUL-15
10094|Lally Conglomerate|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|||||||Fine to coarse grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone and quartz sandstone.|
10094|Lally Conglomerate|69445|6|Mentioned|p30:17|||||||Is overlain by Antrim Plateau Volcanics.||12-JUL-16
10094|Lally Conglomerate|69587|5|Briefly described|500k_geologyp08_lut.csv|Middle Cambrian|Middle Cambrian||||||Basalt with intercalated siliciclastic rocks and chert, basal conglomerate|
10094|Lally Conglomerate|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 2|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|521-505 Ma (Inferred)|||Associated with Antrim Plateau Volcanics.|Fine- to coarse-grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone and quartz sandstone|
10094|Lally Conglomerate|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_interpgeop14_lut.csv.|505-521 Ma|Antrim Plateau Volcanics|||Fine to coarse grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone and quartz sandstone.|
10094|Lally Conglomerate|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Ord Basin.||||||
10094|Lally Conglomerate|71267|4|Described|GEOL_LUT_CSV files|Series 3|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, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|521-505 Ma (inferred)||||Fine- to coarse-grained quartz wacke sandstone, cobble conglomerate, feldspathic sandstone and quartz sandstone|
10094|Lally Conglomerate|72034|6|Mentioned|500k_interpgeop16_lut|Series 3|Series 2|Ord Basin. Mentioned as 'Antrim Plateau Volcanics and Lally Conglomerate'.|||||Siliciclastic sedimentary rocks.|
10097|Lalngang Sandstone|22547|5|Briefly described|p24|||Of Fitzmaurice Group. Overlain by Legune Formation. Correlates with Stonewall Sandstone||||||12-OCT-06
10097|Lalngang Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
10097|Lalngang Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian.||||||12-OCT-06
10097|Lalngang Sandstone|32660|5|Briefly described|Table 6|||||||||
10097|Lalngang Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone, grit, conglomerate, minor siltstone.||||||02-DEC-04
10097|Lalngang Sandstone|32701|4|Described|Table 1|||Fitzmaurice Gp. Adelaidean||||||
10097|Lalngang Sandstone|32728|6|Mentioned|Fig.14|||||||||
10097|Lalngang Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10097|Lalngang Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
10097|Lalngang Sandstone|45112|6|Mentioned|p34|||||||||
10097|Lalngang Sandstone|48938|2|Defined|p16|Adelaidean|Adelaidean|||||||
10097|Lalngang Sandstone|48942|3|Fully described|p36|||Strat. section.||||||
10097|Lalngang Sandstone|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica cemented quartz sandstone, conglomerate, minor siltstone.||||||19-JUL-04
10097|Lalngang Sandstone|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: >1400m. Conformably/disconformably overlies Goobaieri Formation. Grades conformably up into Legune Formation. Geological Province Halls Creek Orogen. Quartz sandstone, conglomerate and minor siltstone.||||||
10097|Lalngang Sandstone|64698|6|Mentioned|lithinterp table|||Also misspelt as Lalngang Sndstone, Laingang Formation, & Lalngang Formation.||||||
10097|Lalngang Sandstone|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cenemnted quartz sandstone, conglomerate, minor siltstone||||||
10097|Lalngang Sandstone|65417|5|Briefly described|p158 Fig.2, p159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Correlated with the Stonewall Sandstone of the Carr Boyd Group (Halls Creek Orogen).||Unit in Fitzmaurice Group.||Is overlain conformably by Legune Formation.||
10097|Lalngang Sandstone|69435|4|Described|p20:2-4|||Sweet et al. (1974). Fitzmaurice Basin. Exposed over a large area. 1400m thick at the type area.||Fitzmaurice Group.||Conformably (?regionally disconformably) overlies Goobaieri Formation. Is overlain gradationally by Legune Formation. Is intruded by Ti Tree Granophyre.|Silica-cemented quartz sandstone, commonly thickly bedded with locally abundant cross-beds and ripple marks; conglomerate, and minor siltstone. Becomes more argillaceous to the NW.|12-JUL-16
10097|Lalngang Sandstone|69673|5|Briefly described|p59, p60 fig 48|||1400m thick.||Fitzmaurice Group||Overlain by Legune Formation, overlies Goobaieri Formation|Silica cemented quartz sandstone, conglomerate and minor siltstone.|
10097|Lalngang Sandstone|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, conglomerate and minor siltstone.|
10097|Lalngang Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
10126|Lampe Formation|41751|6|Mentioned|p8|||||||||
10126|Lampe Formation|44143|4|Described|p.430 Table 4-19; p.452, Figure 4-113|Eocene|Eocene|Up to 2m thick; sandstone and conglomerate; fluvial. Unconformably overlies Paterson and Samuel Formations and Bejah Claystone. Type section at Mount Johnson (HERBERT: 25 deg 24' S, 124 deg 25' E) in the Officer Basin.||||||
10126|Lampe Formation|65102|4|Described|p.366, Figure 4-41, p.369, Table 4-15|Eocene|Eocene|Officer Basin. 2-5m; poorly sorted sandstone & pebble conglomerate; minor siltstone & claystone; fluvial, probably also colluvial; disconformable on older fine-grained units; type section at Mount Johnson (25deg 24min S, 124deg 25min E); unfossiliferous, probably Eocene.||||||
10126|Lampe Formation|65301|5|Briefly described|p5 Fig. 4|Late Cretaceous|Late Cretaceous|Geological province: Canning Basin.||||||
10126|Lampe Formation|65449|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|||||||
10126|Lampe Formation|68007|6|Mentioned|p4|Late Cretaceous|Late Cretaceous|Canning Basin.||||||25-FEB-20
10126|Lampe Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||||
10126|Lampe Formation|69152|4|Described|1m_geologyp08_lut.csv|Cenozoic|Cenozoic||||||Fluvial and probably colluvial poorly sorted sandstone and pebble conglomerate, minor siltstone and claystone.|06-AUG-15
10126|Lampe Formation|70774|5|Briefly described|p4|Late Cretaceous|Late Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||||10-FEB-20
10126|Lampe Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, siltstone, claystone, sandstone|
10126|Lampe Formation|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton.|||||Fluvial and probably colluvial poorly sorted sandstone and pebble conglomerate, minor siltstone and claystone.|
10126|Lampe Formation|73117|5|Briefly described|p3|Upper Cretaceous|Upper Cretaceous|Canning Basin.||||Equivalent[?] to Lake George Formation.|Dominantly sandstone with lesser shale.|
10161|Langfield Group|13194|4|Described|p390 Tb. 4-16, p382 fig 4-59, p399|Tournaisian|Tournaisian|||||Overlies Ningbing Group. Part equivalent to Bonaparte Formation.||
10161|Langfield Group|13234|6|Mentioned|p250 Fig.2, p252 Fig.4,p260 Tb.1, |Early Carboniferous|Early Carboniferous|Potential reservoir.|||||Includes dolomites.|
10161|Langfield Group|14228|5|Briefly described|p6 fig3|Tournaisian|Famennian|Southern Bonaparte Basin.||||Overlies Ningbing Group.||05-OCT-16
10161|Langfield Group|22663|5|Briefly described|W97 8 to 10 fig.2||Carboniferous|||||||01-MAR-10
10161|Langfield Group|23377|6|Mentioned|p212 Fig.5|Carboniferous|Devonian|Of Vulcan Sub-basin.||||||12-OCT-06
10161|Langfield Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.  Max. thickness: 2000 m.||||||
10161|Langfield Group|24390|5|Briefly described|p2 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Sandstone, limestone, shale and siltstone.  Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|24569|5|Briefly described|p248 Fig. 3|Tournaisian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
10161|Langfield Group|40993|2|Defined|p10|Tournaisian|Tournaisian|||||||
10161|Langfield Group|41459|6|Mentioned|Fig.2|||||||||
10161|Langfield Group|41532|6|Mentioned|p292|||||||||
10161|Langfield Group|41598|6|Mentioned|p412|||||||||
10161|Langfield Group|41731|5|Briefly described|p519|||See also p574.||||||12-OCT-06
10161|Langfield Group|41864|4|Described|p101|||Formerly "Eight Mile Creek Group" then "Keep River Group"||||||
10161|Langfield Group|41865|6|Mentioned|Map legend||Tournaisian|||||||
10161|Langfield Group|42442|5|Briefly described|Fig.6 P9|||Same unit as Langfield Group in WA.||||||12-OCT-06
10161|Langfield Group|43236|6|Mentioned|p14,Fig.13.||Tournaisian|||||||
10161|Langfield Group|43661|6|Mentioned|Fig.3|||||||||
10161|Langfield Group|50085|5|Briefly described|p2 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Unconformably overlies Ningbing Group. Sandstone, siltstone, shale, limestone, dolostone.||||||22-JUL-04
10161|Langfield Group|60364|4|Described|p184|Tournaisian|Tournaisian|Alternating calcarenite and sandstone. Overlain by Milligans Formation. Thickness: 900m. Geological Province: Bonaparte Basin.||||||12-OCT-06
10161|Langfield Group|60682|4|Described|piii, 22 Table 5|Tournaisian|Tournaisian|Mixed carbonate/siliciclastic shallow marine deposits. Unconformably overlain by Weaber Group. Max. thickness 900m. Contains 5 formations.||||||31-JUL-15
10161|Langfield Group|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Devonian|Geological Province: Bonaparte Basin.||||||11-APR-08
10161|Langfield Group|61542|5|Briefly described|p277 Fig. 2, p283|Tournaisian|Tournaisian|Includes Bonaparte and Burt Range Formations, Enga Sandstone, Septimus Limestone and Zimmermann Sandstone. Overlies Ningbing Group; unconformably underlies Weaber Group. Geological province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
10161|Langfield Group|62837|5|Briefly described|Stratigraphic columns|Visean|Tournaisian|Includes the Bonaparte Formation.  Age: <355->345Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
10161|Langfield Group|64159|5|Briefly described|p93|Carboniferous|Carboniferous|Contains the Burt Range Formation. Geological Province: Bonaparte Basin.||||||
10161|Langfield Group|64580|4|Described|map legend|Tournaisian|Tournaisian|Undivided; sandstone, limestone,shale and siltstone; includes BONAPARTE (subsurface only) and BURT RANGE FORMATIONS, ENGA and ZIMMERMAN SANDSTONES, and SEPTIMUS LIMESTONE.||||||09-DEC-08
10161|Langfield Group|64689|5|Briefly described|p14, p20|||Gorter et al. (2004) suggest this unit is the source of oil discoveries at Turtle-1 and Barnett-1 (previously thought to be Milligans Formation).||||Overlain unconformably by Milligans Formation.||
10161|Langfield Group|64694|5|Briefly described|p231-233, p234 Fig.2, p236, p238 Tb.1|Visean|Late Tournaisian|See also p239, p241, p242 Tb.4, p243, p246-249.|||Includes Burt Range Formation, Upper Bonaparte Formation, Enga Sandstone, Septimus Limestone and Zimmermann Sandstone.|Overlies Ningbing Group. Overlain by the Weaber Group unconformably.||
10161|Langfield Group|65331|5|Briefly described|Map legend + overview geology map legend|Tournasian|Tournasian|Of Bonaparte Basin. Includes Zimmerman Sandstone, Septimus Limestone, Enga Sandstone, Burt Range Formation. Sandstone, siltstone, shale, limestone, dolostone||||||
10161|Langfield Group|67167|5|Briefly described|Map legend.|Carboniferous|Carboniferous||||||Undivided: shale, siltstone, limestone.|
10161|Langfield Group|67186|5|Briefly described|Map legend.|Carboniferous|Carboniferous||||||Shale, sandstone, limestone.|23-NOV-11
10161|Langfield Group|69099|4|Described|500k_geologyp08_lut.csv|Tournasian|||||Includes Bonaparte (subsurface only) and Burt Range Formations, Enga and Zimmermann Sandstones, and Septimus Limestone.||Sandstone, limestone,shale and siltstone.|31-JUL-15
10161|Langfield Group|69165|4|Described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian||||Includes Bonaparte Formation, Burt Range Formation, Enga Sandstone, Zimmerman Sandstone||Undivided; sandstone, limestone, shale and siltstone|
10161|Langfield Group|69422|6|Mentioned|p7:2 Fig.7.2|Carboniferous|Carboniferous|Bonaparte Basin.||||||12-JUL-16
10161|Langfield Group|69452|4|Described|p36:4, 6-7, 9, 11-13, 15, 18, 23, 28|Early Carboniferous|Late Devonian|Beere and Mory (1986). Petrel Sub-basin, Bonaparte Basin. Up to 900m thick. Non-commercial discoveries of oil and/or gas in the southern part of the Sub-basin are probably sourced from older units of this Group.|||Enga, Zimmerman Sandstones; Burt Range, Bonaparte Formations; Septimus Limestone.|Overlies Ningbing Group conformably or disconformably. Is overlain unconformably by Weaber Group and by Border Creek and Keep Inlet Formations (Kulshill Group).||12-JUL-16
10161|Langfield Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian||||Includes Bonaparte and Burt Range formations, Enga and Zimmerman sandstones, and Septimus Limestone.|||
10161|Langfield Group|69653|5|Briefly described|p10, 14|Carboniferous|Carboniferous|Petrel Sub-basin. Shallow-marine to non-marine settings.||||Overlies Ningbing Group. Is overlain by Weaber Group.|Fine-grained clastic and carbonate sediments.|
10161|Langfield Group|69673|5|Briefly described|p167, p170 fig 142, p171, p177,|Early Carboniferous|Late Devonian|Conventional petroleum potential, sealed by the Milligans Formation, forms a seal for the underlying Ningbing Group. Maximum thickness of 900m.|||Includes Enga Sandstone, Bonaparte Formation, Burt Range Formation, Septimus Limestone, Zimmerman Sandstone|Overlies Ningbing Group, Buttons Formation, overlain by Milligans Formation|Marine sandstone, limestone and shale.|
10161|Langfield Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2|||See also Regional geology: Fig.8, p5, p8-9, p11-12, p16. An equivalent unit in the Petrel Sub-basin includes the upper (Tournaisian) part of the Bonaparte Formation; oil- and gas-prone mudstones, previously assigned to the Milligans Formation.|||Burt Range, Ningbing Limestones.|Is overlain by Milligans Formation.||12-JUL-16
10161|Langfield Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Tournaisian|Tournaisian||346-358 Ma||||Sandstone, limestone, shale, and siltstone|
10161|Langfield Group|70206|5|Briefly described|Map Legend, cross-sect.|Carboniferous|Carboniferous|Bonaparte Basin.|||Includes Zimmerman Sandstone, Septimus Limestone, Enga Sandstone, Burt Range Formation.|Unconformably overlies Ningbing Group. Unconformably overlain by Weaber Group.||
10161|Langfield Group|70812|6|Mentioned|p30|||||||||
10161|Langfield Group|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||||
10161|Langfield Group|70851|6|Mentioned|p17|||||||||
10161|Langfield Group|71146|5|Briefly described|p6,  p43 fig 33|Tournaisian|Famennian|Bonaparte Basin.||||Overlies the Buttons Formation. Unconformably overlain by the Weaber Group.|Sandstone and carbonate.|
10161|Langfield Group|71267|5|Briefly described|1M_geologyp12_lut.csv|Tournaisian|Tournaisian|Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma). See 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|358.9-346.7 Ma (biostrat-inferred)||Includes Burt Range Formation, Enga Sandstone, Hardman Formation, Septimus Limestone, Zimmermann Sandstone.|||
10161|Langfield Group|72034|5|Briefly described|500k_interpgeop16_lut|Tournaisian|Tournaisian|Southern Bonaparte Basin. Max  age from biostratigraphy, min age inferred.|||||Sandstone, limestone, shale, and siltstone.|
10184|Larapinta Group|9199|5|Briefly described|Map legend|Ordovician|Cambrian|Includes the Pacoota Sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|13995|5|Briefly described|p69|Ordovician|Ordovician|Amadeus Basin.|||Stairway Sandstone.|||
10184|Larapinta Group|22561|6|Mentioned|p11|||||||||
10184|Larapinta Group|22563|6|Mentioned|p47||Ordovician|||||||
10184|Larapinta Group|22566|5|Briefly described|p76|Devonian|Late Cambrian|||||||
10184|Larapinta Group|22650|6|Mentioned|Fig 2 on p 157|Ordovician|Cambrian|||||||
10184|Larapinta Group|22651|6|Mentioned|p 189|||||||||
10184|Larapinta Group|22655|6|Mentioned|p 255|||informally divided in to upper and lower Larapinta Group, p255.||||||17-JAN-07
10184|Larapinta Group|22656|6|Mentioned|Fig 4 on p 282|Ordovician|Cambrian|||||||
10184|Larapinta Group|22760|5|Briefly described|p339|||||||||
10184|Larapinta Group|22761|6|Mentioned|Fig 2 on p351|Ordovician||||||||
10184|Larapinta Group|22763|6|Mentioned|p394|Late Ordovician|Cambrian|||||||
10184|Larapinta Group|22804|4|Described|p451|Early Devonian|Late Cambrian|||||||
10184|Larapinta Group|22805|6|Mentioned|p471|||||||||
10184|Larapinta Group|22806|6|Mentioned|p485||Ordovician|||||||
10184|Larapinta Group|22807|6|Mentioned|Fig 3 on p495|Late Ordovician|Early Ordovician|||||||
10184|Larapinta Group|22824|5|Briefly described|p525|Ordovician|Cambrian|||||||
10184|Larapinta Group|22826|6|Mentioned|Fig 4 on p567|||||||||
10184|Larapinta Group|23858|6|Mentioned|p914|||Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||24-MAR-05
10184|Larapinta Group|24301|5|Briefly described|p20|Ordovician|Ordovician|Includes Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone.   Geological Province: Amadeus Basin||||||
10184|Larapinta Group|24302|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes the Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|29721|6|Mentioned|Table 44|||||||||
10184|Larapinta Group|29972|6|Mentioned|p4|||Upper Cambrian- Ordovician||||||
10184|Larapinta Group|30238|4|Described|p64|||Cambrian - Ordovician age.||||||17-JAN-07
10184|Larapinta Group|30258|6|Mentioned|Fig.2|||Ordovician age||||||
10184|Larapinta Group|30544|6|Mentioned|p49|||||||||
10184|Larapinta Group|30817|6|Mentioned|p14|||||||||
10184|Larapinta Group|31566|6|Mentioned|p230|||Ordovician||||||
10184|Larapinta Group|31567|6|Mentioned|p280|||Unconformably overlain by Langra Formation.||||||17-JAN-07
10184|Larapinta Group|31707|4|Described|p50|||Discussed.||||||17-JAN-07
10184|Larapinta Group|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
10184|Larapinta Group|33192|6|Mentioned|p20|||||||||
10184|Larapinta Group|33307|6|Mentioned|Fig.6|||||||||
10184|Larapinta Group|33738|6|Mentioned|p52|||||||||
10184|Larapinta Group|33761|6|Mentioned|p146|||Ord.- Sil? - Dev.||||||
10184|Larapinta Group|33971|5|Briefly described|p28|||Strat. section Fig.15.||||||
10184|Larapinta Group|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also pp15-18.||||||13-OCT-06
10184|Larapinta Group|34186|6|Mentioned|Fig.4|||Ordovician||||||
10184|Larapinta Group|34442|5|Briefly described|Table 1|||Cambrian - Ordovician. See also pp8,9,10,11.||||||13-OCT-06
10184|Larapinta Group|34488|6|Mentioned|p11|||||||||
10184|Larapinta Group|34579|4|Described|Table 2|||Cambrian - Ordovician. See pp10,15,16.||||||13-OCT-06
10184|Larapinta Group|34580|4|Described|Table 1|||Ordovician||||||
10184|Larapinta Group|35102|6|Mentioned|p4|||||||||
10184|Larapinta Group|36198|6|Mentioned|Fig.III.2|||||||||
10184|Larapinta Group|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
10184|Larapinta Group|36643|6|Mentioned|p65|||||||||
10184|Larapinta Group|36818|6|Mentioned|p203|||||||||
10184|Larapinta Group|36821|6|Mentioned|p397|||||||||
10184|Larapinta Group|38329|6|Mentioned|p210|||||||||
10184|Larapinta Group|38606|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|38885|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian - Early Ordovician||||||
10184|Larapinta Group|39565|6|Mentioned|p33|||||||||
10184|Larapinta Group|39583|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|39931|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
10184|Larapinta Group|40136|5|Briefly described|p29|||||||||
10184|Larapinta Group|40201|5|Briefly described|Table 1|||||||||
10184|Larapinta Group|40740|3|Fully described|p46|||Mention p6.||||||13-OCT-06
10184|Larapinta Group|40810|4|Described|p7|||||||||
10184|Larapinta Group|41018|6|Mentioned|p236|||||||||
10184|Larapinta Group|41039|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41115|6|Mentioned|p1400|||||||||
10184|Larapinta Group|41190|6|Mentioned|p267|||||||||
10184|Larapinta Group|41203|5|Briefly described|p4|||||||||
10184|Larapinta Group|41224|5|Briefly described|p430|||||||||
10184|Larapinta Group|41270|6|Mentioned|p272|||||||||
10184|Larapinta Group|41385|6|Mentioned|Fig.3|||||||||
10184|Larapinta Group|41621|5|Briefly described|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41711|6|Mentioned|p259|||||||||
10184|Larapinta Group|41717|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|41723|6|Mentioned|Map legend|Ordovician||||||||
10184|Larapinta Group|41801|5|Briefly described|p212|||||||||
10184|Larapinta Group|41819|6|Mentioned|Map legend|Late Ordovician|Late Cambrian|||||||
10184|Larapinta Group|41820|5|Briefly described|p7|||||||||
10184|Larapinta Group|42060|6|Mentioned|Fig.5 P140|||||||||
10184|Larapinta Group|42082|6|Mentioned|p322|||||||||
10184|Larapinta Group|42141|6|Mentioned|Fig.3 P570|||||||||
10184|Larapinta Group|42354|5|Briefly described|p3, p6|||Defined by Prichard and Quinlan (1962).||||||17-JAN-07
10184|Larapinta Group|42504|6|Mentioned|p77|||||||||
10184|Larapinta Group|42699|5|Briefly described|map legend|Ordovician||||||||
10184|Larapinta Group|42940|5|Briefly described|Plate 2|Ordovician|Ordovician|Siltstone, sandstone, limestone, dolostone, phosphorite; marine fossils.  Age: 500-440Ma. Geological province: Amadeus Basin.||||||23-JAN-08
10184|Larapinta Group|43035|5|Briefly described|p21|||||||||
10184|Larapinta Group|43105|5|Briefly described|Fig.3,p8.|||||||||
10184|Larapinta Group|43225|5|Briefly described|Map Legend||Ordovician|In the Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|43503|6|Mentioned|32-50|Silurian|Late Cambrian|||||||
10184|Larapinta Group|43631|6|Mentioned|p26|||||||||
10184|Larapinta Group|43647|6|Mentioned|Fig.4,533|||||||||
10184|Larapinta Group|43648|5|Briefly described|Fig.1,p488|||||||||
10184|Larapinta Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
10184|Larapinta Group|43817|6|Mentioned|Fig.1,p42|||||||||
10184|Larapinta Group|44133|5|Briefly described|p43|||Includes: Stairway Sandstone.||||||
10184|Larapinta Group|44323|14|Not recorded|map legend||Ordovician|SG/53-6. Ordovician.||||||
10184|Larapinta Group|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
10184|Larapinta Group|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
10184|Larapinta Group|44393|6|Mentioned|p.7|||refs Wells et al 1968.||||||
10184|Larapinta Group|44395|14|Not recorded|p.8,9,12,13, Tb.2|||||||||
10184|Larapinta Group|44402|5|Briefly described|map legend|Ordovician|Cambrian|Includes Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone. Camb-Ord.||||||02-DEC-04
10184|Larapinta Group|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
10184|Larapinta Group|44484|14|Not recorded|p.3,5,10,Fig.4,Tb.1|Ordovician|Cambrian|Camb-Ord. See also p.12,14, for more details.||||||
10184|Larapinta Group|44485|14|Not recorded|map legend|Ordovician|Cambrian|Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Carmichael Sandstone, Stokes Siltstone. Camb-Ord.||||||
10184|Larapinta Group|44493|4|Described|p.11||Ordovician|BLOODS RANGE sheet (G53-3). See p.8,13, for details.||||||22-DEC-09
10184|Larapinta Group|44494|14|Not recorded|map legend||Ordovician|||||||
10184|Larapinta Group|44497|4|Described|p.10-11, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
10184|Larapinta Group|44498|14|Not recorded|map legend|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44505|14|Not recorded|p.2,7,8,10,11, Fig 1|Ordovician|Cambrian|Camb-Ord.||||||
10184|Larapinta Group|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian-Ordovician.||||||
10184|Larapinta Group|45036|6|Mentioned|p3|||Upper Cambrian - Upper Ordovician age||||||
10184|Larapinta Group|45041|4|Described|p61|||See also pp62-86. Ordovician.||||||13-OCT-06
10184|Larapinta Group|45118|6|Mentioned|p3|||||||||
10184|Larapinta Group|45155|6|Mentioned|p36|||See also Fig.37||||||
10184|Larapinta Group|45170|6|Mentioned|Fig.8|||||||||
10184|Larapinta Group|46829|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|46856|6|Mentioned|p279|||||||||
10184|Larapinta Group|46928|6|Mentioned|Table 1|||||||||
10184|Larapinta Group|47050|6|Mentioned|Fig.2|||||||||
10184|Larapinta Group|47052|6|Mentioned|p261|||||||||
10184|Larapinta Group|48639|14|Not recorded|p.16,opp.p.1|Ordovician|Cambrian|Ord-Cam. (G55-2).||||||
10184|Larapinta Group|48838|2|Defined|p.18,22, Tb.1,2|||||||||
10184|Larapinta Group|48862|14|Not recorded|p.1,18,24-29,39-42|||(F52-15). Pl.10,11.||||||
10184|Larapinta Group|48863|14|Not recorded|p.30||Ordovician|Tb.1. opp.p.7,p.2,7,12,24,30,31,37,39-42,Pl.11,13,15,16. (G52-4,G53-1).||||||
10184|Larapinta Group|48864|2|Defined|p.32||Ordovician|Tb.1. On many pages. p.2,9,10,27,38,30,34,37,47,50,Pl.11. (G52-3). Ord.||||||
10184|Larapinta Group|48865|4|Described|p.23||Ordovician|Includes: Pacoota Sandstone, Horn Valley Fm, Stokes Fm, Stairway Sandstone. Ord. On many pages. p.20,21,27,45-47,50,Pl.8.||||||
10184|Larapinta Group|48880|14|Not recorded|p.20,33,Pl.10,11||Ordovician|(F53-13,F53-14). Ord.||||||
10184|Larapinta Group|48890|4|Described|p.44-47|Ordovician|Cambrian|See also Tables, Figs and Plates. Camb-Ord.||||||13-OCT-06
10184|Larapinta Group|48963|6|Mentioned|p2|||p22||||||13-OCT-06
10184|Larapinta Group|50098|5|Briefly described|p1|Ordovician|Late Cambrian|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|50286|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60547|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60572|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated, minor siltstone, and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|60674|5|Briefly described|Map legend|Ordovician|Cambrian|Includes: Pacoota Sandstone, Horn Valley and Stokes Siltstones, and Carmicahel Sandstone.  Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|60678|5|Briefly described|Map legend|Ordovician|Ordovician|White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.  Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60679|5|Briefly described|Map Legend|Ordovician|Ordovician|Sandstone, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|60683|4|Described|p26, p9 Tb. 1|Ordovician|Ordovician|White sandstone, locally bioturbated, with minor siltstone and conglomeratic sandstone. Geological Province: Musgave Block/ Amadeus Basin.||||||16-JUN-09
10184|Larapinta Group|60904|5|Briefly described|p790 Fig. 16|Middle Ordovician|Late Cambrian|Marine sediments.||||||
10184|Larapinta Group|61386|5|Briefly described|Map legend|Cambrian|Cambrian|White sandstone, locally bioturbated, minor siltstone and conglomeratic sandstone. Geological Province: Amadeus Basin.||||||23-DEC-09
10184|Larapinta Group|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway and Carmichael Sandstones. Geological Province: Amadeus Basin.||||||17-JAN-07
10184|Larapinta Group|61518|5|Briefly described|Map Legend|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62376|5|Briefly described|p18|Early Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||09-FEB-10
10184|Larapinta Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Late Cambrian|Geological Province: Amadeus Basin.||||||
10184|Larapinta Group|62609|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite. Underlies: Mereenie Sandstone. Overlies: Pertaoorrta Group.||||||14-AUG-06
10184|Larapinta Group|62620|5|Briefly described|Map Legend|Ordovician|Cambrian|Siltstone, sandstone, limestone, dolomite, phosphorite.||||||
10184|Larapinta Group|62794|5|Briefly described|p288, p289 Fig.2, p290|Ordovician|Late Cambrian|In Amadeus Basin, southern Northern Territory. Over 2100 m thick. Comprises (in ascending order) Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.||||||
10184|Larapinta Group|62982|5|Briefly described|p7|Late Ordovician|Late Cambrian|Includes the Pacoota Sandstone at its base. Thick marine deposits. Geological Province: Amadeus Basin. Hosts two producing oil and gas fields.||||||16-JAN-07
10184|Larapinta Group|63562|6|Mentioned|p348-349|Middle Ordovician|Late Cambrian|Of Amadeus Basin.|||Includes Pacoota and Stairway Sandstones, and Horn Valley and Stokes Siltstones.|||
10184|Larapinta Group|64334|5|Briefly described|p37, 40, 42, 45, 47|Ordovician|Late Cambrian|Prichard and Quinlan (1962). Originally the Larapintine Series of Tate (1896), using the Aboriginal name for the Finke River. Mostly shallow-marine. Up to 2300m thick.|||Pacoota, Carmichael Sandstones; Horn Valley, Stairway, Stokes Siltstones.|Unconformably overlies Pertaoorrta Group.||
10184|Larapinta Group|64778|6|Mentioned|p12-13|Ordovician|Ordovician|Amadeus Basin. Post-Delamerian Orogeny sediments; thickening to N; over 2000m.||||||
10184|Larapinta Group|64809|6|Mentioned|p3 Fig.2, p6 Fig.4 |Early Devonian|Proterozoic||||Includes the Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||
10184|Larapinta Group|64970|6|Mentioned|p719 Fig. 2|Silurian|Ordovician|Geological Province: Amadeus Basin.||||||27-MAY-09
10184|Larapinta Group|65102|6|Mentioned|p363, Figure 4-38|Paleozoic|Paleozoic|Amadeus Basin.||||||
10184|Larapinta Group|65233|3|Fully described|p3 Fig. 2, p9|Silurian|Late Cambrian|Informally divided into Lower - Upper Larapinta Groups; upper comprises Carmichael and Mereenie Sandstones; lower consists of Pacoota and Stairway Sandstone, and Horn Valley and Stokes Siltstones. Unconformably overlies Goyder Formation. In Amadeus Basin.||||||16-JUL-13
10184|Larapinta Group|65256|5|Briefly described|p6 Tb.1, p24, p16, p19|Ordovician|Ordovician|White to red sandstone, locally bioturbated, minor siltstone, conglomeratic sandstone and limestone interbeds; fossiliferous. Onlaps Dean Quartzite; unconformably overlies Pottoyu Granite Suite; may directly overlie basement; locally overlies Winnall beds. Some sections contain angular clasts of Dean Quartzite. Includes Stokes Siltstone. >10m thick.||||||
10184|Larapinta Group|65272|6|Mentioned|p319, p320 Fig.3|Ordovician|Cambrian|Northern Amadeus Basin. Thick marine sequences coeval with the Larapinta Event.||||||
10184|Larapinta Group|65489|5|Briefly described|p125|Ordovician|Cambrian|Amadeus Basin.|||Includes Pacoota, Stairway and Carmichael Sandstones; Horn Valley and Stokes Siltstones.|Overlies Pertaoorrta Group.||
10184|Larapinta Group|66767|5|Briefly described|p60|Ordovician|Ordovician|NE Amadeus Basin.|||Horn Valley Siltstone.|Overlies Pertaoorta Group. Is overlain by Mereenie Sandstone.|Predominantly siliciclastic sedimentary rocks.|
10184|Larapinta Group|67326|5|Briefly described|p2-3|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|Overlies Pertaoorrta Group. Is overlain by Pertnjara Group.||
10184|Larapinta Group|67565|5|Briefly described|p5 Fig.3, pp41-42.|||Amadeus Basin.|||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||03-DEC-15
10184|Larapinta Group|67856|5|Briefly described|p338 fig 4-30|Late Ordovician|Late Cambrian||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone.|||
10184|Larapinta Group|68316|6|Mentioned|p779, p785|Ordovician|Ordovician|Amadeus Basin.||||||
10184|Larapinta Group|68323|6|Mentioned|p4 Fig.2|Early Devonian|Late Cambrian|Amadeus Basin.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|69438|5|Briefly described|p23:2-5, 7-8, 20, 32-39, 46, 50, 60|Late Ordovician|Late Cambrian|Defined, as were its constituent Formations, by Pritchard and Quinlan (1962); after the Larapintine Series of Tate (1896). They included sandstone of the Carmichael Sandstone in the upper Stokes Siltstone (others mapped it as lower Mereenie Sandstone). Amadeus Basin.|||Pacoota, Stairway, Carmichael Sandstones; Horn Valley, Stokes Siltstones.|Is overlain disconformably by Dare Siltstone Member (Parke Siltstone).||12-JUL-16
10184|Larapinta Group|69444|6|Mentioned|p29:6|Ordovician|Ordovician|Amadeus Basin. Deposition was coincident with tectonism (the Larapinta Event) with peaks at 475 Ma and 460 Ma.||||||12-JUL-16
10184|Larapinta Group|69449|5|Briefly described|p34:4|Ordovician|Ordovician|Amadeus Basin.|||Pacoota Sandstone.|||12-JUL-16
10184|Larapinta Group|69458|6|Mentioned|p42:8|Ordovician|Ordovician|Amadeus Basin.||||||12-JUL-16
10184|Larapinta Group|69606|5|Briefly described|p4 fig 2|Ordovician|Cambrian|Misspelling of the Larapinta Group. Amadeus Basin. The carbonate shales and muds are potential source and seal rocks whilst the sandstones are potential reservoir rocks.||||Unconformably overlies the Upper Pertaoorta Group. Overlain by the Carmichael Sandstone.|Interbedded sandstone, carbonate, shale and marl.|
10184|Larapinta Group|69673|6|Mentioned|p66, p102, p103||||||Includes Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|70749|6|Mentioned|p54|||Amadeus Basin.|||Pacoota Sandstone.|||
10184|Larapinta Group|71146|5|Briefly described|p6|Wenlock|Cambrian|Amadeus Basin.|||Includes the Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and the Carmichael Sandstone.|Unconformably overlies the Pertaoorrta Group.|Sandstone, carbonate, mudstone and coal.|
10184|Larapinta Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10184|Larapinta Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Marine sediments. White sandstone, locally bioturbated; minor siltstone and conglomeratic sandstone.|
10184|Larapinta Group|71279|5|Briefly described|p355 Fig.2, p363, p365, p374, p382 Tb.1|Early Devonian|Late Cambrian|Amadeus Basin. Modelled magnetic properties.|||Pacoota, Stairway, Carmichael, Mereenie Sandstones; Horn Valley, Stokes Siltstones.|||
10184|Larapinta Group|71898|5|Briefly described|iii, p1, p3, p17, p20-p22|||Amadeus Basin. Outcrops on the PALM VALLEY Sheet (5440) of the HENBURY Sheet (SG 53-01).|||Includes the Horn Valley Siltstone and the Pacoota Sandstone.|Overlies the Pertaoorrta Group.||19-NOV-18
10184|Larapinta Group|71965|6|Mentioned|p911|||Of Amadeus Basin.||||Correlable to Warratta Group.||
10184|Larapinta Group|72360|5|Briefly described|Map legend|Ordovician|Cambrian|Of Amadeus Basin.|||Includes Carmichael Sandstone, Stairway Sandstone, Horn Valley Siltstone and Pacoota Sandstone.|||09-SEP-19
10184|Larapinta Group|72369|5|Briefly described|iii,26,37|Devonian|Ordovician|Of Amadeus Basin.|||Includes Pacoota and Stairway sandstones, Stokes Siltstone, and the Carmichael and Mereenie sandstones, Parke Siltstone, Horn Valley Siltstone.|||
10184|Larapinta Group|72374|5|Briefly described|iii,p3,17|||Of Amadeus Basin.|||Layout implies includes Carmichael and Mereenie sandstones.|||11-OCT-19
10184|Larapinta Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
10184|Larapinta Group|73085|6|Mentioned|p1, p4|early Devonian|late Cambrian||||Mereenie Sandstone, Carmichael Sandstone, Stokes Siltstone, Stairway Sandstone, Horn Valley Siltstone, Pacoota Sandstone.|||
10184|Larapinta Group|73119|6|Mentioned|piii, p19|||Amadeus Basin, western.|||Stairway Sandstone|||
10184|Larapinta Group|73279|6|Mentioned|p10-14|Ordovician|Cambrian|Amadeus Basin.|||Pacoota Sandstone, Stairway Sandstone, Stokes Siltstone, Carmichael Sandstone|||
10184|Larapinta Group|73437|6|Mentioned|p152|||Apatite fission track cooling age of 341+/-58 Ma from Tingate, (1990).||||||
10253|Lawlers Tonalite|23159|6|Mentioned|p805|Archean|Archean|||||||07-NOV-08
10253|Lawlers Tonalite|23926|5|Briefly described|p28|||||||||
10253|Lawlers Tonalite|24174|5|Briefly described|p30|||Geological Province: Eastern Goldfields.||||||
10253|Lawlers Tonalite|24196|5|Briefly described|p52|Archean|Archean|Age: 2666 +/- 3 Ma (Fletcher et al., 1998)||||||07-NOV-08
10253|Lawlers Tonalite|24494|6|Mentioned|p21|||See also "Lawlers Tonalite"||||||
10253|Lawlers Tonalite|35113|6|Mentioned|Table.1|||Also Table.2,Sr ratios and dates. Described P56,petrology.||||||
10253|Lawlers Tonalite|35681|6|Mentioned|p42|||||||||
10253|Lawlers Tonalite|37795|6|Mentioned|Table 4|||||||||
10253|Lawlers Tonalite|38512|6|Mentioned|Table III|||||||||
10253|Lawlers Tonalite|38979|6|Mentioned|Table 3|||||||||
10253|Lawlers Tonalite|39469|6|Mentioned|p250|||||||||
10253|Lawlers Tonalite|41886|5|Briefly described|p169|||||||||
10253|Lawlers Tonalite|41887|6|Mentioned|p186|||||||||
10253|Lawlers Tonalite|42156|6|Mentioned|p374|||||||||
10253|Lawlers Tonalite|43595|6|Mentioned|p228|||Intrusion at 2652+/-20 Ma||||||
10253|Lawlers Tonalite|43776|6|Mentioned|p325|||Rb-Sr Whole rock: 2652+/-20 Ma||||||
10253|Lawlers Tonalite|44149|6|Mentioned|p111 Fig.2-120|||Agnew area, Eastern Goldfields Province.||||||
10253|Lawlers Tonalite|60416|5|Briefly described|p21|Archean|Archean|Coarse-grained and comprises zoned plagioclase phenocrysts in groundmass of feldspar, quartz, biotite and amphibole; xenoliths locally abundant, and leucogranite veins cut the tonalite in places. Age: 2666+/-3Ma (U-Pb, Fletcher et al 1998) and 2666+/-7Ma.||||||07-NOV-08
10253|Lawlers Tonalite|69583|5|Briefly described|p73, p89-90, p92, p94, p150, p170, p172|Archean|Archean|See also Plates 2, 4. Beneath the Lawlers Anticline. See also references to the informal Lawlers tonalite (p40, p88, p171). Seismic interpretation. Forms a body tapering to the W. May have been a factor in gold mineralisation.|c.2665 Ma (Champion, writtten comm., 2013).||||A large, dome-shaped granitic unit (modelled).|
10253|Lawlers Tonalite|69586|5|Briefly described|p11|||Lawlers Anticline. Syntectonic. Hosts gold mineralisation (Lawlers and Great Eastern deposits).|c.2666 Ma (Dunphy et al., 2003).|||||
10253|Lawlers Tonalite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2665 +/- 4 Ma (isotopic).||||Tonalite, quartz diorite, and granodiorite; metamorphosed.|
10253|Lawlers Tonalite|70326|5|Briefly described|p337-338|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Intruded into lower sections of the Lawlers Antiform and Mount White Synform.|2666+\-3 Ma (Fletcher et al., 1988).||||Quartz diorite to tonalite and granodiorite.|
10253|Lawlers Tonalite|70420|6|Mentioned|p9 Fig.6|Archean|Archean|||||||
10253|Lawlers Tonalite|71212|4|Described|p69, p73, p74, p75, p144, p147|Neoarchean|Neoarchean|Yilgarn Craton. Hosts the Daisy Queen gold deposit. A Rb-Sr age by Cooper et al, 1978 is 2652+/-20 Ma is provided as is an age of 2661 +/-23 Ma (U-Pb whole rock).  See also p82-p86, p88, p90, p91, p113-p116, p118, p158, p186, p195, p198, p230, p232, p240, p242, p244, p245, p248, App B tbl B1, tbl B2.|2665 +/- 35 Ma (Rb-Sr)|||Probably equivalent to the Camel Bore Granodiorite.|Medium-grained, hornblende-biotite tonalite to medium-grained, mesocratic and granoblastic granodiorite with subordinate biotite-quartz diorite.|
10253|Lawlers 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).|2665 Ma (inferred)||||Tonalite, quartz diorite, and granodiorite; metamorphosed|
10253|Lawlers Tonalite|73151|5|Briefly described|p2-3, p5, p11, p16|Neoarchean|Neoarchean|Yilgarn Craton. Intrudes stratigraphy of the Agnew Greenstone Belt, situated in the core of the Lawler Anticline. Divided by Foden et al., (1984) into three geochemical groups. Cut by leucogranite dykes that are ca. 2666 Ma (Fletcher et al., 2001), 2628 +/- 21 Ma age for monzonite on the edge of the Lawlers Tonalite (Thebaud et al., 2018). Written as Lawlers tonalite on p11.|ca 2690 Ma, 2668 Ma||||Includes an older foliated tonalite, as well as younger massive granodiorite-granite and a fine-crystalline, dyke-forming leucogranite.|
10253|Lawlers Tonalite|73238|5|Briefly described|p12, 13 Fig.10, 15, 27|||A small, sub-circular intrusion at the northern margin of the Agnew granitic complex. Eastern Goldfields Terrane.|2665 +/- 4 Ma (Fletcher et al., 2001).|||||
10253|Lawlers Tonalite|73596|6|Mentioned|p1151, 1157-1158|Neoarchean|Neoarchean|Lawlers Domain, Agnew-Wiluna Greenstone Belt.|2666 +/- 3 Ma.|||||
10274|Le Lievre Formation|42710|5|Briefly described|map legend|Proterozoic||Variation on Le Lievre Beds.||Of Oscar Range Group.||||17-OCT-12
10274|Le Lievre Formation|42811|4|Described|p28|||of Oscar Range Group. Base of Fm not seen. Exposed thickness ~800 m.||||Overlain, slightly unconformably by Ellendale Formation|Red-brown to grey phyllite with minor sandstone interbeds, overlain by massive thick-bedded, medium to coarse-grained quartzite and quartz sandstone, with monor phyllite. Magnetite-bearing phylite at top..|17-OCT-12
10274|Le Lievre Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Oscar Range Group.|||Red-brown to grey phyllite with minor sandstone interbeds near the base, overlain by massive, thickly bedded, rippled and cross-bedded medium to coarse grained quartzite and quartz sandstone with minor phyllite|
10282|Learmonth Formation|14227|5|Briefly described|p11|Late Jurassic|Middle Jurassic|Geological Province: Exmouth Sub-basin. Non-marine to marine sands.||||||07-FEB-11
10282|Learmonth Formation|23815|4|Described|p292|Late Jurassic|Middle Jurassic|Geological Province: Carnarvon Basin. Overlying unit: Wogatti Sandstone (unconformable). Underlying unit: Lyons Group or Callytharra Formation (both unconformable). Max. thickness: 674 m.||||||27-APR-05
10282|Learmonth Formation|24059|5|Briefly described|p138|Jurassic|Jurassic|Geological Province: Exmouth Sub-basin.||||||
10282|Learmonth Formation|24351|5|Briefly described|Plate 4 (in pocket)|Early Jurassic|Early Jurassic|Geological Province: Exmouth Sub-basin.||||||13-DEC-07
10282|Learmonth Formation|31561|5|Briefly described|p34|||Stratigraphy. Marginal to non marine.||||||
10282|Learmonth Formation|32648|6|Mentioned|p32|||Jur.||||||
10282|Learmonth Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
10282|Learmonth Formation|33386|6|Mentioned|Fig.7|||||||||
10282|Learmonth Formation|33435|6|Mentioned|p134|||Jurassic.||||||
10282|Learmonth Formation|33453|4|Described|p71|||||||||
10282|Learmonth Formation|34134|6|Mentioned|Cor.Chart|||Lower - Upper Jurassic||||||
10282|Learmonth Formation|34838|6|Mentioned|Fig.3|||||||||
10282|Learmonth Formation|35282|6|Mentioned|Fig.2|||||||||
10282|Learmonth Formation|35983|6|Mentioned|Table 27|||||||||
10282|Learmonth Formation|36112|6|Mentioned|p31|||||||||
10282|Learmonth Formation|36257|6|Mentioned|Table 2.1|||||||||
10282|Learmonth Formation|36890|3|Fully described|p292|||||||||
10282|Learmonth Formation|37364|6|Mentioned|p1050|||||||||
10282|Learmonth Formation|38732|6|Mentioned|p31|||||||||
10282|Learmonth Formation|39427|4|Described|Table 1|||||||||
10282|Learmonth Formation|41271|3|Fully described|p124|||||||||
10282|Learmonth Formation|41436|6|Mentioned|p46|||||||||
10282|Learmonth Formation|41438|6|Mentioned|p106|||||||||
10282|Learmonth Formation|41440|4|Described|p136|||||||||
10282|Learmonth Formation|41443|6|Mentioned|Fig.4|||||||||
10282|Learmonth Formation|41444|6|Mentioned|Fig.4|||||||||
10282|Learmonth Formation|41446|6|Mentioned|Fig.17|||||||||
10282|Learmonth Formation|41751|6|Mentioned|p4|||||||||
10282|Learmonth Formation|42615|4|Described|p37|||Name has become functionally useless.||||||
10282|Learmonth Formation|45015|5|Briefly described|map legend|Late Jurassic|Late Jurassic|Known only in bores. Geological Province: Carnarvon Basin.||||||31-MAY-06
10282|Learmonth Formation|45016|14|Not recorded|p47||Jurassic|Fig 56.||||||
10282|Learmonth Formation|49942|6|Mentioned|p40|||||||||03-FEB-05
10282|Learmonth Formation|60384|6|Mentioned|p243 Fig 2b, p261|Late Jurassic|Early Jurassic|Northern Carnarvon Basin. Potential reservoir.||||||
10282|Learmonth Formation|61958|5|Briefly described|Map sheet 1|Late Jurassic|Late Jurassic|||||||21-MAR-06
10282|Learmonth Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Early Jurassic|Age: ~200-180Ma. Geological Province: Northern Carnarvon Basin.||||||01-MAR-10
10282|Learmonth Formation|63950|5|Briefly described|p336 Fig. 4|Late Jurassic|Early Jurassic|Overlies Murat Siltstone and Athol Formation, with which it also interfingers; underlies Calypso Formation. Geological Province: northern Carnarvon Basin.||||||01-FEB-10
10282|Learmonth Formation|67195|5|Briefly described|Appendix 2, p7|||Carnarvon Basin.|||||Includes cream medium-grained sandstone.|21-SEP-18
10282|Learmonth Formation|69182|6|Mentioned|Ch3 p23-p26, Ch3 p53, Ch3 p71|Jurassic|Jurassic|||||||
10282|Learmonth Formation|69558|6|Mentioned|p258 fig 419|Jurassic|Jurassic|||||Overlain by the Wogatti Sandstone. Faulted against the Lyons Group.||
10282|Learmonth Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Is overlain by Calypso Formation.||
10282|Learmonth Formation|70066|5|Briefly described|Regional: Fig.6|Aalenian|Sinemurian|Exmouth Sub-basin, Northern Carnarvon Basin.||||Overlies and is interbedded with Murat Siltstone. Is overlain by and interbedded with Athol Formation.||
10282|Learmonth Formation|73564|6|Mentioned|p1225|Jurassic|Jurassic|Cuvier Margin.||||Correlated with Calypso Formation, and Athol Formation with Dingo Claystone.||
10291|Leederville Formation|12758|5|Briefly described|p22, P3 Fig. 3|Late Cretaceous|Early Cretaceous|Of the Warnbro Group. Sandstone, shale, conglomerate. Directly overlies the Parmelia Group in Parmelia 1 drillhole. Unconformably overlain by the Coolyena Group; underlain by the South Perth Shale. Max. thickness: 663m. Geol.Prov: Perth Basin.||||||28-JUL-09
10291|Leederville Formation|12759|3|Fully described|p35; p28 Tb. 7; p32 Fig 15.|Aptian|Valanginian|Defined Cockbain and Playford (1973). Type section in the Leederville Valley (Redan Street) bore (198-433 m). Max thickness onshore is 600m at Yanchep synclinal axis. Overlain unconformably by Osborne Formation, Molecap Greensand and Gingin Chalk. Forms a major confined aquifer.||Of Warnbro Group.|Includes (this study) Mariginiup, Wanneroo and Pinjar Members.|Overlies (unconformably) Cattamarra Coal Measures, Yarragadee or Parmelia Formations, and (conformably) Gage Formation and South Perth Shale. See Comments.|Discontinuous, interbedded sandstones, siltstones and shales with some conglomerate to the east.|12-MAY-14
10291|Leederville Formation|14227|5|Briefly described|Enclos. 2|Early Cretaceous|Early Cretaceous|Of Warnbro Group. Presented as Leederville Fm.||||||07-FEB-11
10291|Leederville Formation|22742|5|Briefly described|p116, p118 Fig. 3|Early Cretaceous|Early Cretaceous|Unconformably underlies Tamala Limestone.||||||05-NOV-14
10291|Leederville Formation|22820|3|Fully described|p12 Fig. 5, p22|Cretaceous|Cretaceous|Of Warnbro Group. Unconformably overlies Willespie Fm and Rosabrook C.M. Thickness: up to 300m. Geolprov: S. Perth Basin. Interbedded, poorly consolid'd, fine- to coarse-gr. sst.+ black, carbonaceous shale and distinctive glauconitic shale + lignite seams||||||28-JUL-09
10291|Leederville Formation|23279|5|Briefly described|p30|||||||||
10291|Leederville Formation|23816|4|Described|p246|Aptian|Neocomian|Formerly known as the "Leederville Sandstone". Geological Province: Perth Basin. Of the Warnbro Group. Underlying unit: South Perth Shale (conformable). Overlying unit: Kings Park Shale (unconformable). Max. thickness: 545 m.||||||
10291|Leederville Formation|23880|6|Mentioned|p41|||Geological Province: Perth Basin.||||||
10291|Leederville Formation|24160|6|Mentioned|p88-89, p95, p96|Early Cretaceous|Early Cretaceous|Text specifies "consists of the lower South Perth Shale and the upper Leederville Formation"; [what happens to the rest of these units?]. Important source of structural clay for Perth.||||Unconformably overlies Yarragadee Formation. Is overlain unconformably by Dandaragan Sandstone or Osborne Formation.|Interbedded sandstone, shale, siltstone and claystone; minor conglomerate.|
10291|Leederville Formation|24443|5|Briefly described|Fig.31|Early Cretaceous|Early Cretaceous|Of Warnbro Group. Overlies South Perth Shale. Unconformably overlain by Coolyena Group. Geological Province: Perth Basin.||||||03-FEB-05
10291|Leederville Formation|29382|6|Mentioned|Table 10|||||||||
10291|Leederville Formation|29693|6|Mentioned|Fig.7|||||||||
10291|Leederville Formation|30217|6|Mentioned|p25|||Correlation.||||||
10291|Leederville Formation|31153|5|Briefly described|p10|||Refers bivalve content||||||
10291|Leederville Formation|31238|4|Described|p27|||||||||
10291|Leederville Formation|33747|6|Mentioned|p1072|||||||||
10291|Leederville Formation|35093|6|Mentioned|p22|||||||||
10291|Leederville Formation|35100|6|Mentioned|p165|||||||||
10291|Leederville Formation|35638|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10291|Leederville Formation|35968|5|Briefly described|p64|||Hydrogeology on P65.||||||
10291|Leederville Formation|35970|5|Briefly described|p77|||Discussion re hydrogeology.||||||
10291|Leederville Formation|35973|5|Briefly described|p94|||||||||
10291|Leederville Formation|35983|6|Mentioned|Table 26|||||||||
10291|Leederville Formation|36257|6|Mentioned|Table 2.1|||||||||
10291|Leederville Formation|36265|5|Briefly described|Fig.3.26|Early Cretaceous|Early Cretaceous|Of the Warnbro Group. Geological province: Perth Basin.||||||04-MAR-08
10291|Leederville Formation|36293|2|Defined|p169|Aptian|late Neocomian|Late Neocomian to Aptian.||||||
10291|Leederville Formation|36890|3|Fully described|p247|||Formerly Leederville Sandstone||||||
10291|Leederville Formation|37104|6|Mentioned|Fig.3|||||||||
10291|Leederville Formation|37309|4|Described|p16|||Groundwater p18.||||||14-DEC-22
10291|Leederville Formation|38479|6|Mentioned|p15|||||||||
10291|Leederville Formation|38777|3|Fully described|p29|||||||||
10291|Leederville Formation|38778|4|Described|p15|||||||||
10291|Leederville Formation|39156|4|Described|p22|||||||||
10291|Leederville Formation|39211|6|Mentioned|p61|||See also P62,66||||||
10291|Leederville Formation|39554|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10291|Leederville Formation|39794|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10291|Leederville Formation|39829|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10291|Leederville Formation|39834|4|Described|p288|||||||||
10291|Leederville Formation|39915|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10291|Leederville Formation|40304|3|Fully described|p39|||||||||
10291|Leederville Formation|40305|4|Described|p78|||||||||
10291|Leederville Formation|40348|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10291|Leederville Formation|40358|4|Described|p23|||||||||
10291|Leederville Formation|40359|4|Described|p22|||||||||
10291|Leederville Formation|40395|6|Mentioned|p333|||||||||
10291|Leederville Formation|40902|6|Mentioned|p55|||||||||
10291|Leederville Formation|41057|6|Mentioned|p82|||||||||
10291|Leederville Formation|41346|6|Mentioned|p19|||||||||
10291|Leederville Formation|41634|6|Mentioned|p42|||||||||
10291|Leederville Formation|41728|6|Mentioned|Fig.3|||||||||
10291|Leederville Formation|41751|6|Mentioned|p6|||||||||
10291|Leederville Formation|41780|5|Briefly described|p2|||||||||
10291|Leederville Formation|41781|4|Described|p11|||||||||
10291|Leederville Formation|41782|4|Described|p23|||See also P29||||||
10291|Leederville Formation|41783|4|Described|p41|||||||||
10291|Leederville Formation|41985|3|Fully described|p63|||||||||
10291|Leederville Formation|41986|5|Briefly described|p34|||||||||
10291|Leederville Formation|41989|4|Described|p113|||||||||
10291|Leederville Formation|42194|4|Described|p61|||||||||
10291|Leederville Formation|42434|6|Mentioned|p6|||||||||
10291|Leederville Formation|42687|6|Mentioned|map legend|||||||||
10291|Leederville Formation|42688|6|Mentioned|map legend|Cretaceous||||||||
10291|Leederville Formation|42711|6|Mentioned|p30|||Geological province: Perth Basin. Approximately equivalent to Nakina Formation in the Collie Basin.||||||28-JUL-09
10291|Leederville Formation|42734|5|Briefly described|map legend|Cretaceous||||||||
10291|Leederville Formation|43031|5|Briefly described|Fig.2.|||||||||
10291|Leederville Formation|43062|5|Briefly described|p23,Table 2,p18|||||||||
10291|Leederville Formation|43068|6|Mentioned|p138|||||||||
10291|Leederville Formation|43096|5|Briefly described|Fig.2|||||||||
10291|Leederville Formation|43197|5|Briefly described|Map Legend||Cretaceous|of Warnbro Group.||||||
10291|Leederville Formation|43347|4|Described|9|Aptian|Valanginian|||||||
10291|Leederville Formation|44144|4|Described|p504 Tb.4-21, p516-517|Aptian|Hauterivian|Type Section: Leederville Valley (Redan Street) bore; 31o56'09''S 115o50'07''E 198-433m.  545m thick shallow marine and paralic deposits.||Warnbro Group||Overlies South Perth Shale transitionally. Overlain by Osborne Formation, Molecap Greensand (both disconformably); Rockingham Sand, Porpoise Bay Formation (unconformably).|Fine grained sandstone, shale, siltstone and claystone; minor conglomerate.|
10291|Leederville Formation|45104|6|Mentioned|p35|||||||||
10291|Leederville Formation|45168|6|Mentioned|p6|||||||||
10291|Leederville Formation|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Of the Warnbro Group. Overlain unconformably by Coolyena Group. Underlain by South Perth Shale.||||||07-FEB-11
10291|Leederville Formation|60556|5|Briefly described|p24, p25 Fig. 15|Mesozoic||Mesozoic||||||
10291|Leederville Formation|61811|5|Briefly described|p3 Fig.2, p55 Table 7, p57.|Early Cretaceous|Early Cretaceous|Northern Perth Basin.||Unit in Warnbro Group.||Overlies South Perth Shale. Is overlain by Molecap Greensand, Poison Hill Greensand and, locally, by Gingin Chalk.||
10291|Leederville Formation|64580|4|Described|map legend||Early Cretaceous|Of Warnbro Group. Interbedded sandstone and siltstone; minor conglomerate; scattered thin coal seams.||||||09-DEC-08
10291|Leederville Formation|64635|5|Briefly described|p4 Fig.3 |Barremian|Hauterivian|||Of the Warnbro Group.||Overlies South Perth Shale.||
10291|Leederville Formation|65306|5|Briefly described|p20, p21 (fig)|Early Cretaceous|Early Cretaceous|Unconformably overlies the Yarragadee Formation and its aquifer.||||||10-SEP-09
10291|Leederville Formation|67115|4|Described|p63-75|Middle Cretaceous|Early Cretaceous|Perth Basin. Compositional variation and provenance investigated using major and trace element geochemistry, mineralogy and grain size relationships. Up to 600 m thick. Sourced from local granitoids from the Yilgarn Craton.||Warnbro Group.|Mariginiup, Wanneroo and Pinjar Members.|Conformably overlies the South Perth Shale; underlies the Osborne Formation.|Poorly to well-sorted interbedded sandstones, siltstones and mudstones. Pyrite and uncharacterized carbonaceous material, glauconite.|
10291|Leederville Formation|67135|5|Briefly described|p5 Fig.7, p32, p33 Fig.42, p58.|Cretaceous|Cretaceous|Perth Basin. Hosts aquifer used for Perth's potable water supply. Source of brick-making clay near Muchea and Bullsbrook.||||Overlies South Perth Shale. Is overlain by Coolyena Group.||
10291|Leederville Formation|67340|6|Mentioned|p6, 8-9, 25, 50, 52, 55, 60, 62|Early Cretaceous|Early Cretaceous|Northern Perth Basin. Wells in this unit used for this Report are listed.||||Overlies South Perth Shale.||
10291|Leederville Formation|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Aptian|Hauterivian|||Warnbro Group||Unconformably overlain by the Osborne Formation. Unconformably overlies the Bunbury Basalt.||
10291|Leederville Formation|68254|5|Briefly described|p1036 Fig.2, p1037 Tb.2, p1040 Tb.3|Cretaceous|Cretaceous|||Of the Warnbro Group.|Includes Pinjar Member, Wanneroo Member, and Mariginiup Member.|||
10291|Leederville Formation|68811|4|Described|p92 fig 52, p93-p95, p97|Cretaceous|Cretaceous|Deposited in an onshore fluvial or swamp environment. Hosts the Leederville aquifer and contains six distinct members. See also p98 fig 56, p154 app 1, p155 app 1, p180 tbl 39.|||Includes the Pinjar, Wanneroo, Maringiniup and Henley Sandstone Members.|Overlies the South Perth Shale. Unconformably overlies the Cockleshell Gully Formation and the Yarragadee Formation. Overlain by the Kardinya Shale and the Lancelin Formation.|Interbedded sandstone, siltstone, shale and minor conglomerate and coal seams.|
10291|Leederville Formation|69081|5|Briefly described|p736 Tb.1|Early Cretaceous|Early Cretaceous|Presented as Leederville Fm in figure. Geol. Prov: Perth Basin||Warnbro Group||is unconformably overlain by Osborne Formation; overlies South Perth Shale||
10291|Leederville Formation|69182|6|Mentioned|Ch2 p3, Ch2 p9, Ch2 p55, Ch2 p57|Lower Cretaceous|Lower Cretaceous|Perth Basin.||Warnbro Group||Overlies the South Perth Shale. Overlain by the Dandaragan Sandstone.||
10291|Leederville Formation|69297|6|Mentioned|p174, p175, p189|Cenomanian|Hauterivian|Vlaming Sub-basin. Deposited in a deep marine or deltaic environment.||Warnbro Group||Overlies the South Perth Shale. Overlain by the Osborne Formation.||
10291|Leederville Formation|70097|5|Briefly described|p19 Fig.3|Aptian|Barremian|Southern Perth Basin. Mandurah Terrace and Vlaming Sub-basin.||Warnbro Group||Overlies South Perth Shale. Is overlain by Coolyena Group.|Includes siltstone.|12-SEP-17
10291|Leederville Formation|70099|5|Briefly described|Fig.4; p6|Aptian|Hauterivian|Vlaming Sub-basin. Correlated to Mentelle 6 and 7A Supersequences.||Warnbro Group.||Overlies South Perth Shale. Is overlain by Osborne Formation (Coolyena Group).|Interbedded marine sandstones and mudstones.|
10291|Leederville Formation|70128|5|Briefly described|p449, p451, p456, p458-462|Early Cretaceous|Early Cretaceous|Southern and central Perth Basin. Thickness varies from 0 to 1200m. Modelled thickness distribution histogram.||Warnbro Group.||Conformably overlies South Perth Shale. Is overlain unconformably by Coolyena Group.||
10291|Leederville Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, claystone, siltstone|
10291|Leederville Formation|71377|4|Described|p1-p3, p7, p9-p14|Aptian|Valanginian|Perth Basin. SHRIMP age is interpreted as the maximum depositional age derived from detrital zircons in this study. SHRIMP age is consistent with the biostratigraphic age of Early Cretaceous. Intersected in GSWA Harvey 1 (53-249m) in which it is described. Interpreted to consist of mainly shallow-marine to fluvial deposits. Zircon morphology and sample descriptions are provided. See also p17, p85, p87-p88, p90, p103.|134 +/- 3 Ma (SHRIMP U-Pb)|Warnbro Group||Conformably overlies the South Perth Shale. Unconformably overlies the Eneabba Formation. Unconformably overlain by the Osborne Formation.|Poorly consolidated, interbedded, fine to coarse-grained sandstone and shale with distinctive glauconitic shale and lignite seams.|
10291|Leederville Formation|71958|6|Mentioned|p34-p36, p41, p53-p54, p60-p61|||Vlaming Sub-basin. Initially proposed by Fairbridge (1953). Davidson (1995) sub-divided it further into three units and a summary of its lithostratigraphy was found in Crostella and Backhouse (2000). Part of this unit in the northern Vlaming Sub-basin has been seperated and reclassified out as part of the South Perth Supersequence.||Warnbro Group|||Shallow marine sandstones.|
10291|Leederville Formation|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Hauterivian|Perth Basin.  Age from biostratigraphy.||Warnbro Group|||Interbedded sandstone and siltstone; minor conglomerate; scattered thin coal seams.|
10291|Leederville Formation|72258|5|Briefly described|p129,133,137|Early Cretaceous|Early Cretaceous|Of Perth Basin. Deposited soon after breakup of Austral-Antarctica and greater India. Dominated by Neoarchean detrital zircons, with minor Neoproterozoic grains and subordinate Mesoproterozoic input compared to the rest of the Perth Basin, suggestive of greater influence from primary detritus delivery than sediment recycling. 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). 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. 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).||||Underlain by South Perth Shale, or unconformably by Bubury Basalt.||
10291|Leederville Formation|73424|6|Mentioned|p5|Early Cretaceous|Early Cretaceous|Perth Basin.||||||
10296|Leeuwin Complex|12758|6|Mentioned|p2 Figs. 1 & 2, p9|||||||||
10296|Leeuwin Complex|22554|6|Mentioned|p550.1|||||||||
10296|Leeuwin Complex|22635|6|Mentioned|p482||Proterozoic|||||||
10296|Leeuwin Complex|22716|5|Briefly described|table4, p239|Neoproterozoic|Neoproterozoic|Intruded at 780Ma, 680Ma, 540Ma. Deformation and metamorphism at 620 Ma.||||||
10296|Leeuwin Complex|22786|5|Briefly described|p30|||||||||
10296|Leeuwin Complex|22812|6|Mentioned|p627, p630||Neoproterozoic|||||||
10296|Leeuwin Complex|22814|6|Mentioned|p257|||||||||
10296|Leeuwin Complex|22818|6|Mentioned|map|||||||||
10296|Leeuwin Complex|22819|6|Mentioned|map|||||||||
10296|Leeuwin Complex|22820|6|Mentioned|p3, p6, p7 Fig. 3|||||||||11-AUG-08
10296|Leeuwin Complex|23150|6|Mentioned|p24|||of Perth Basin.||||||
10296|Leeuwin Complex|23727|5|Briefly described|p4 Fig 1.|||||||||
10296|Leeuwin Complex|23788|3|Fully described|p17|Early Paleozoic|Neoproterozoic|See also p6.||||||07-NOV-08
10296|Leeuwin Complex|23914|5|Briefly described|p159|Neoproterozoic|Neoproterozoic|Geological Province: Yilgarn Craton.||||||
10296|Leeuwin Complex|24160|6|Mentioned|p23, p92|Proterozoic|Proterozoic|Pinjarra Orogen.||||||
10296|Leeuwin Complex|24170|5|Briefly described|p711|Phanerozoic|Neoproterozoic|Geological Province : Yilgarn Craton||||||
10296|Leeuwin Complex|24197|5|Briefly described|p108|||Consists of intensely deformed plutonic igneous rocks, mainly granite metamorphosed to granulite facies. Rocks at Cape Leeuwin have been dated as 688+/-7Ma and 681+/-10Ma; granite gneiss at Cosy Corner at 779+/-23Ma.||||||07-FEB-11
10296|Leeuwin Complex|24410|6|Mentioned|p37, p42 Fig. 8|||Geological Province: Perth Basin.||||||
10296|Leeuwin Complex|24522|6|Mentioned|p80 Fig. 2|Neoproterozoic|Neoproterozoic|||||||
10296|Leeuwin Complex|24524|6|Mentioned|p193|||||||||
10296|Leeuwin Complex|24526|5|Briefly described|p106 Fig. 7, p113|Proterozoic|Proterozoic|Dominated by felsic orthogneiss, ranging from granodiorite to alkali granite in composition, interleaved with anorthosite, leucogabbro and subordinate mafic lenses.  See also p112 Fig. 9, p114.||||||
10296|Leeuwin Complex|24542|5|Briefly described|p2 Fig.2, p5|Neoproterozoic|Mesoproterozoic|Granitic orthogneiss, granite, amphibolite, geniss, migmatic, gneiss.||||||
10296|Leeuwin Complex|24595|4|Described|p585, p586 Fig. 1a|Cambrian|Mesoproterozoic|Geological Province: Pinjara Orogen.||||||
10296|Leeuwin Complex|42069|5|Briefly described|p241|||||||||
10296|Leeuwin Complex|43030|5|Briefly described|Map Legend|||||||||
10296|Leeuwin Complex|43038|5|Briefly described|p9|||||||||
10296|Leeuwin Complex|43189|5|Briefly described|Map Legend||Proterozoic|||||||
10296|Leeuwin Complex|43212|4|Described|P4,P5,p7.||Proterozoic|Rb-Sr age of c.655 Ma. U-Pb SHRIMP zircon age of c.560 Ma.||||||
10296|Leeuwin Complex|43251|6|Mentioned|Fig 8.11,p131||Proterozoic|see also p136,Fig 8.12,p132 & p137||||||
10296|Leeuwin Complex|43442|6|Mentioned|p48|||May be a geological province rather than stratigraphic name.||||||
10296|Leeuwin Complex|43561|6|Mentioned|p1443|||||||||
10296|Leeuwin Complex|43573|6|Mentioned|p314||Proterozoic|||||||
10296|Leeuwin Complex|44138|4|Described|p264 Fig.3-54, p265, p266-271|||Sm-Nd model age (Fletcher, 1988). Also 655 +/- 25 Ma (Compston and Arriens, 1968) age from a mixed whole-rock and mineral Rb-Sr isochron reflects low-grade metamorphism.|1.48 to 1.13 Ga.||Augusta Anorthosite Complex||Intensely deformed plutonic igneous rocks, mainly granite, metamorphosed in granulite facies: coarse-grained granulite, basic granulite, medium-grained granulite, all intruded by granite (gneiss); anorthosite-gabbro intrusions.|
10296|Leeuwin Complex|49942|6|Mentioned|p37|||||||||
10296|Leeuwin Complex|50008|5|Briefly described|p48|Neoproterozoic|Neoproterozoic|Gneissic Inlier. Intensely deformed orthogneiss, anorthosite, and minor metabasite, metamorphosed to granulite facies. Age of zircon populations given. Geological Province: Pinjarra Orogen||||||15-JUN-05
10296|Leeuwin Complex|50228|6|Mentioned|p479 Fig.2|||||||||
10296|Leeuwin Complex|50428|6|Mentioned|p1.1|||||||||
10296|Leeuwin Complex|50543|5|Briefly described|Map|||Structural term in this context.||||||
10296|Leeuwin Complex|50620|6|Mentioned|p22|||Of the Pinjarra Orogeny. Age: 500Ma (Nelson, 1996, 1999, 2000, 2001 and 2002).||||||
10296|Leeuwin Complex|50621|6|Mentioned|p158 Fig. 1|||Geological Province: Pinjarra Orogen.||||||
10296|Leeuwin Complex|60372|6|Mentioned|p85 Fig.1,p87.|Proterozoic|Proterozoic|||||||
10296|Leeuwin Complex|60384|6|Mentioned|p255|||||||||
10296|Leeuwin Complex|60470|6|Mentioned|p5|||SW WA. Includes zircon-bearing rocks of ~1070 Ma.||||||
10296|Leeuwin Complex|60556|5|Briefly described|p2 Fig. 2, p3-4, p29, p34|Proterozoic||||||||
10296|Leeuwin Complex|61023|5|Briefly described|p23|Mesoproterozoic|Mesoproterozoic|||||||
10296|Leeuwin Complex|61564|6|Mentioned|p589 Fig. 1|||Structural term in this context.||||||
10296|Leeuwin Complex|62381|6|Mentioned|p2 Fig.2, p9. |||Pervasive deformation and metamorphism at 550-500 Ma.||||||
10296|Leeuwin Complex|63869|6|Mentioned|p3 Fig.1|||||||||
10296|Leeuwin Complex|64571|6|Mentioned|p838|Cambrian|Neoproterozoic|||||||
10296|Leeuwin Complex|64635|6|Mentioned|p1|||Perth Basin.||||||
10296|Leeuwin Complex|64722|5|Briefly described|Fig. 2 p3-6, p19||Mesoproterozoic|Multiple phases of granitic rock intrusion recognised: 1080 Ma, 800 - 650 Ma, 540 - 535 Ma, 525 Ma.|||||Dominated by felsic orthogneiss with interleaved anorthosite, leucogranite and some mafic lenses.|11-APR-12
10296|Leeuwin Complex|64769|6|Mentioned|p99|Proterozoic|Proterozoic|||||||
10296|Leeuwin Complex|64777|5|Briefly described|p1 Fig.2, p6 |||SHRIMP U-Pb orthogneiss zircon crystallisation ages (Nelson 1999). Zircons in felsic gneiss have ages between 779 and 524 Ma (Nelson 1995).|1091 +/- 8 Ma and 1091 +/- 17 Ma/||||Consists of intensely deformed orthogneiss, anorthosite, and minor metabasite, metamorphised to granulite facies.|
10296|Leeuwin Complex|65306|6|Mentioned|p20 (1st fig.)|||Probably a structural term in this context.||||||10-SEP-09
10296|Leeuwin Complex|65487|6|Mentioned|p2 Fig.1, p57 Fig.28|||||||||
10296|Leeuwin Complex|65664|6|Mentioned|p1099, Fig.3|||Pinjarra Orogen, SW WA.||||||09-MAY-12
10296|Leeuwin Complex|67340|6|Mentioned|p5|||Northern Perth Basin.||||||
10296|Leeuwin Complex|67380|6|Mentioned|p6 Fig.3|||Albany-Fraser Orogen.||||||
10296|Leeuwin Complex|67581|6|Mentioned|p37-38, 48|Early Cambrian|Neoproterozoic|Pinjarra Orogen. Part of Perth Basin basement.|||||Includes gneisses.|
10296|Leeuwin Complex|70097|6|Mentioned|p1|||||||||
10296|Leeuwin Complex|70125|5|Briefly described|p403 Fig.15|||Prydz-Leeuwin Belt, the site of the 570-530 Ma Kuungan Orogeny. Contains rocks aged 1200-1000 Ma and 700-500 Ma.||||||
10296|Leeuwin Complex|70128|6|Mentioned|p454|||Precambrian terrane surrounding shelves of Perth Basin sediments.||||||
10296|Leeuwin Complex|70838|5|Briefly described|p278 Fig.11, p279|Cambrian|Neoproterozoic|Pinjarra Orogen. Age of protolith crystallisation and amphibolite-granulite facies metamorphism (570-500 Ma) shown in Fig.11 (showing detrital zircon age distributions).|760-730 Ma (protolith).|||||
10296|Leeuwin Complex|70879|5|Briefly described|p1, p9, p16-18|Neoproterozoic|Neoproterozoic|Pinjarra Orogen. Previously, only two Mesoproterozoic crustal samples were known (two c.1090 Ma garnet-bearing orthogneisses). Generally has protoliths aged 780-760 Ma with Sm-Nd depleted-mantle model ages of 1600-1100 Ma. This contrasts strongly with these new SHRIMP U-Pb zircon ages (1092 +/- 27 Ma and 1076 +/- 35 Ma) from basement underlying the northern and southern Perth Basin respectively. The latter experienced isotopic resetting at 680 +/- 110 Ma.|780-680 Ma (protoliths).||||Orthogneisses.|
10296|Leeuwin Complex|71999|6|Mentioned|p610 fig 17|||South west WA.|757 - 522 Ma|||||
10296|Leeuwin Complex|72004|6|Mentioned|p76|||~550 - 500 Ma?||||||
10296|Leeuwin Complex|72491|6|Mentioned|p2, 6, 16, 18, 20|||||||||
10296|Leeuwin Complex|73184|6|Mentioned|p196|||Granitoid and dyke intrusions within the Leeuwin Complex have an age of 540-520 Ma, potential source of Neoproterozoic-Cambrian detrital zircons in the Grant Group.|||||Includes granitoid and dyke intrusions.|
10296|Leeuwin Complex|73423|6|Mentioned|p6|Proterozoic|Proterozoic|[Written as Leeuwin complex]. Constitutes crystalline basement in far south-western WA.||||Unconformably overlain by Tamala Limestone.||
10296|Leeuwin Complex|73424|6|Mentioned|p2-3, 6, 8|||Pinjarra Orogen. A promontory forming the western border of the Scott Coastal Plain, WA.  Ages have been recorded at 1100-1000 Ma, 750 Ma, and ~520 Ma.||||||
10296|Leeuwin Complex|73480|6|Mentioned|p203|Cambrian|Ediacaran||ca 550-500 Ma|||||
10296|Leeuwin Complex|73574|6|Mentioned|p761|||||||||
10298|Lefroy Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
10298|Lefroy Formation|22901|6|Mentioned|74|||Geol Province Officer Basin.||||||11-APR-08
10298|Lefroy Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
10298|Lefroy Formation|23571|4|Described|p7|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Underlying Unit: Townsend Quartzite. Overlying Unit: Browne Formation (disconformable?).||||||
10298|Lefroy Formation|24161|4|Described|p9 Fig.6, p30|Neoproterozoic|Neoproterozoic|Unconformably overlies the Townsend Quartzite. Disconformably overlain by the Browne Formation. Geological Province: Officer Basin.||||||
10298|Lefroy Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
10298|Lefroy Formation|41751|6|Mentioned|p8|||||||||
10298|Lefroy Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: <800Ma. Geological Province: Officer Basin.||||||24-SEP-08
10298|Lefroy Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.||Unit in Buldya Group.||Overlies Townsend Quartzite conformably and locally unconformably.|Shale, mudstone.|
10298|Lefroy Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
10298|Lefroy Formation|61272|5|Briefly described|p123 Fig.4|||Unconformably overlies Townsend Quartzite. Unconformably overlain by Browne Formation.||||||
10298|Lefroy Formation|61732|5|Briefly described|p4 Fig. 3, p85|Willouran|Willouran|Disconformably overlain by Lupton Formation. Geological Province: central Officer Basin.||||||07-FEB-11
10298|Lefroy Formation|62453|3|Fully described|p5 Fig. 3, 17|Cryogenian|Cryogenian|Of the Buldya Group. Geological Province: Officer Basin. Conformably overlies: Townsend Quartzite. Formerly Lefroy Beds. Unconformably underlies: Lupton Formation. Siltstone, sandstone. Age: 825-800Ma.||||||
10298|Lefroy Formation|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
10298|Lefroy Formation|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
10298|Lefroy Formation|64325|5|Briefly described|p82 Fig. 2|Neoproterozoic|Neoproterozoic|A unit of Supersequence 1. Conformably overlies Townsend Quartzite; overlain by Browne Formation. Geological Province: western Officer Basin. Shale/mudstone unit. Comprises marine sandstone, siltstone and shale.||||||
10298|Lefroy Formation|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.||||||09-DEC-08
10298|Lefroy Formation|64793|6|Mentioned|p283-286, p291 fig 8|Cryogenian|Cryogenian|Of central Officer Basin. Age inferred from Fig.3.|c.840-c.836 Ma.|||||
10298|Lefroy Formation|64970|5|Briefly described|p718, p719 Fig. 2|Riphean|Riphean|In places is underlain by Townsend Quartzite. Consists of fine sandstones, siltstones and grey marine shales. Geological Province: Officer Basin.||||||
10298|Lefroy Formation|65102|4|Described|p365, 366,367,372, Figs.4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. 250-500?m; siltstone & fine sandstone with minor claystone; marine, below wave base deposition; conformable on Townsend Quartzite, disconformably overlain by Lupton Formation; type section in Ainslie Gorge, 26deg 14min S, 126deg 38min E; unfossiliferous.||||||
10298|Lefroy Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||Unit in Buldya Group.||||
10298|Lefroy Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group, central Officer Basin||||||
10298|Lefroy Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group, central Officer Basin||||||
10298|Lefroy Formation|65416|5|Briefly described|p137, p140, p145.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Sequence LP1A of Supersequence PL1. Crops out along the southwest margin of the Musgrave Complex. Correlated with Jilyili Formation in the Savory Sub-basin; marine and marine-modified delta regressive deposition.||||Overlies Townsend Quartzite conformably/gradationally. Is overlain unconformably by Lupton and Browne Formations.|Sandstones, siltstones and marine shales.|
10298|Lefroy Formation|66281|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.|||||Laminated to very thickly-bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
10298|Lefroy Formation|66282|6|Mentioned|Map legend.|||Officer Basin. No outcrop on map; interpreted bedrock geology only.||||||
10298|Lefroy Formation|67195|5|Briefly described|p9 fig 5, p10, p19 tbl 1,p20, 45, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 1.61 W/mK. Regarded as deep water equivalent of the Townsend Quartzite. Total thickness 19m in Empress 1A, the only well in this study to intersect this unit. See also App 1, App 2.||||Overlies Townsend Quartzite, unconformably overlain by Browne Formation.|Heavily fractured maroon to grey siltstone; shale and mudstone.|05-JAN-23
10298|Lefroy Formation|67200|5|Briefly described|app 2 p10||||||||Heavily fractured siltstone.|
10298|Lefroy Formation|67244|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin. Described together with Townsend Quartzite.||Unit in Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|15-AUG-18
10298|Lefroy Formation|68270|5|Briefly described|p678|||Western Officer Basin.||||Overlain disconformably by Lupton Formation.||
10298|Lefroy Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
10298|Lefroy Formation|69029|6|Mentioned|p329|Neoproterozoic|Neoproterozoic|Of Officer Basin.||||Overlain by Browne Formation. Underlain by Townsend Quartzite.||
10298|Lefroy Formation|69091|5|Briefly described|p34|||In GSWA Empress 1A, Stevens and Apak (1999) interpreted interval of mixed mudstone and mafic volcanic unit (from 1521.8 m to 1540 m) as Lefroy Formation, a unit near base of Officer Basin succession, above siliciclastic and volcanic rocks interpreted as being pre-Officer Basin (1540-1624 m, TD). Re-examination of the core indicated that all the section below 1521.8 m is part of Mesoproterozoic basement (Grey et al., 2005).||||||07-OCT-14
10298|Lefroy Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Officer Basin, Centralian Superbasin. Lithology description shared with Townsend Quartzite.||Buldya Group|||Quartz arenite and feldspathic arenite; minor conglomerate and shale beds|
10298|Lefroy Formation|70634|4|Described|500k_geolgyp08_lut.csv|Neoproterozoic|Neoproterozoic|Included with Townsend Quartzite in file.||Buldya Group|||Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
10298|Lefroy Formation|70793|5|Briefly 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_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.||Unit of Buldya Group.||||
10298|Lefroy Formation|71268|5|Briefly described|100k_interpgeop_lut.csv|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.||Unit of Buldya Group.||Underlain by Townsend Quartzite.||
10301|Legendre Formation|12498|6|Mentioned|p517 Fig.3. |Middle Jurassic|Middle Jurassic|||||Is overlain by Calypso Formation.||
10301|Legendre Formation|23726|5|Briefly described|p8 Fig 2c|Middle Jurassic|Early Jurassic|Overlying unit Angel Formation. Underlying unit North Rankin Formation. Geological Province: Carnarvon Basin.||||||
10301|Legendre Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
10301|Legendre Formation|29721|6|Mentioned|Table 102|||||||||
10301|Legendre Formation|31604|6|Mentioned|p6|||Bajocian to Oxfordian. (Dingo Gp.) See also Table 14.||||||
10301|Legendre Formation|32711|6|Mentioned|Fig.3|||||||||
10301|Legendre Formation|32714|6|Mentioned|Fig.7|||Jurassic. Dingo Gp.||||||
10301|Legendre Formation|32715|6|Mentioned|Fig.16|||||||||
10301|Legendre Formation|33386|6|Mentioned|Fig.7|||||||||
10301|Legendre Formation|33453|6|Mentioned|p71|||M.-U.Jur.||||||
10301|Legendre Formation|40617|2|Defined|p9|Middle Jurassic|Early Jurassic|Early to Middle Jurassic||||||01-SEP-14
10301|Legendre Formation|41271|3|Fully described|p128|||||||||
10301|Legendre Formation|41438|6|Mentioned|p106|||||||||
10301|Legendre Formation|41440|6|Mentioned|p136|||||||||
10301|Legendre Formation|41445|6|Mentioned|Fig.4|||||||||
10301|Legendre Formation|41732|6|Mentioned|p534|||||||||
10301|Legendre Formation|42116|5|Briefly described|Fig.1 P6|||||||||
10301|Legendre Formation|42615|3|Fully described|p31|Callovian early|Toarcian late|||||||
10301|Legendre Formation|42822|5|Briefly described|p110|||||||||
10301|Legendre Formation|43712|6|Mentioned|p11|||||||||
10301|Legendre Formation|43722|6|Mentioned|p10|||||||||
10301|Legendre Formation|43724|6|Mentioned|p29|||||||||
10301|Legendre Formation|43825|6|Mentioned|p147|Middle Jurassic|Early Jurassic|Dampier Sub-basin||||||
10301|Legendre Formation|43826|6|Mentioned|Fig.2,p163||Middle Jurassic|||||||01-MAR-10
10301|Legendre Formation|43828|6|Mentioned|p202|||Canning and Browse basins||||||
10301|Legendre Formation|46950|6|Mentioned|Fig.15|||||||||
10301|Legendre Formation|50085|5|Briefly described|p23 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin.||||||
10301|Legendre Formation|60379|5|Briefly described|p126 fig 3, p128, 130, p133-138, 140|Bathonian|Bathonian|Dampier sub-basin, Carnarvon Basin. Hydrocarbon play sealed by Calypso Formation. Shown as Upper Legendre Formation p135, Lower Legendre Formation p136.||||||
10301|Legendre Formation|60386|6|Mentioned|p300, p302|Middle Jurassic|Early Jurassic|Northern Carnarvon Basin. Deltaic-nearshore-shelf||||||
10301|Legendre Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Early Jurassic|Age: ~190-~164Ma. Geological Province:  Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
10301|Legendre Formation|63950|5|Briefly described|p336 Fig. 4, p337|Late Jurassic|Early Jurassic|Overlies Murat Siltstone and Athol Formation, with which it also interfingers; underlies Calypso Formation. Geological Province: northern Carnarvon Basin. Contains deltaic and near-shore sands.||||||27-MAY-08
10301|Legendre Formation|64978|6|Mentioned|p528 Fig.2.|Middle Jurassic||Part of Perseus hydrocarbon reservoir is the Bathonian sandstone in this unit.||||||
10301|Legendre Formation|64979|6|Mentioned|p541, pp547-548|Middle Jurassic|Middle Jurassic|Hydrocarbon reservoir in Reindeer Field, Dampier Sub-basin.||||||
10301|Legendre Formation|66126|6|Mentioned|p206|Middle Jurassic|Middle Jurassic|Carnarvon Basin.||||||
10301|Legendre Formation|67200|5|Briefly described|p8 fig 6, |Jurassic|Jurassic|||||Overlies North Rankin Formation, overlain by Angel Formation|Sandstone and siltstone with some limestone.|
10301|Legendre Formation|67368|5|Briefly described|p209 Fig.4.|Middle Jurassic|Middle Jurassic|Hosts a gross gas column of c.151 m TVD, intersected by the Persephone-1 well. Is juxtaposed, across the major North Rankin Field bounding fault, against the North Rankin Beds and the Mungaroo Formation.||||Overlies Athol Formation. Is overlain by Calypso Formation.|Fluvial and marine deltaic sandstones; minor shale.|
10301|Legendre Formation|68054|6|Mentioned|p41-42|Middle Jurassic|Early Jurassic|Northern Carnarvon Basin. Penetrated by the Perseus-3A well; palynomorphs therein are a focus of this article. Abundant photographs; systematic palaeontology of dinoflagellate cysts.|||||Fluviodeltaic and marginal marine sandstones.|
10301|Legendre Formation|68135|5|Briefly described|p51 fig 2a|Bathonian|Pliensbachian|Northern Carnarvon Basin.||||Overlies Athol Formation. Is overlain by Calypso Formation.||14-SEP-17
10301|Legendre Formation|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|||Carnarvon Basin. See also Ch3 p23, Ch3 p35, Ch3 p65-p66, Ch3 p73.||||||
10301|Legendre Formation|69297|6|Mentioned|p339, p352|||Beagle Sub-basin of the Northern Carnarvon Basin.||||||
10301|Legendre Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||||
10301|Legendre Formation|70065|6|Mentioned|Regional: p5|||Beagle Sub-basin.||||Part-equivalent to Depuch Formation.||
10301|Legendre Formation|70066|5|Briefly described|Dampier: Fig.2; p1-2. Exmouth: Fig.2; p2|Callovian|Bajocian|See also Regional: Fig.6; p5, p8-9. Northern Carnarvon Basin. Gas source in the Reindeer and Saffron-Rosemary accumulations from fluvio-deltaic sediments. Likely source of Legendre-Jaubert and Sage oil accumulations in the Dampier Sub-basin, and others in southern Beagle Sub-basin. Fluvio-deltaic to marine sediments are potential reservoirs with intraformational seals.||||Overlies Athol Formation. Is overlain by Calypso Formation.|Regressive deltaic sandstone.|
10303|Legune Formation|22547|5|Briefly described|p24|||Of Fitzmaurice Group. Overlies Lalngang Formation. Correlates with Pincombe Formation||||||13-OCT-06
10303|Legune Formation|32307|4|Described|Table 2|||Proterozoic||||||
10303|Legune Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
10303|Legune Formation|32660|5|Briefly described|Table 6|||||||||
10303|Legune Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone and siltstone.||||||02-DEC-04
10303|Legune Formation|32701|4|Described|Table 1|||Adelaidean. See also p7. Of Fitzmaurice Gp.||||||13-OCT-06
10303|Legune Formation|32728|6|Mentioned|Fig.14|||||||||
10303|Legune Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10303|Legune Formation|37462|6|Mentioned|Fig.4.13|||||||||
10303|Legune Formation|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10303|Legune Formation|40494|4|Described|p11|||||||||
10303|Legune Formation|41645|6|Mentioned|p15|||||||||
10303|Legune Formation|45112|6|Mentioned|Table 16|||||||||
10303|Legune Formation|48938|2|Defined|p19|Proterozoic|Proterozoic|See also pp20-21. Measured section p88.||||||13-OCT-06
10303|Legune Formation|48942|3|Fully described|p37|||||||||
10303|Legune Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica cemented quartz sandstone, siltstone.||||||
10303|Legune Formation|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: >600m. Overlies Lalngang Formation (conformable) and Whitewater Volcanics (unconformable). Geological Province: Halls Creek Orogen. Medium grained quartz sandstone, siltstone, fine grained sandstone.||||||04-MAY-05
10303|Legune Formation|64698|4|Described|lithinterp table|||Age ~1150-1250Ma (Stenian) but age name given as Statherian.Of Fitzmaurice Group. Max. thickness 600m. Silica cemented quartz sandstone, siltstone. Conformably overlies Lalngang Sandstone (and other misspellings).||||||07-JAN-09
10303|Legune Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cemented quartz sandstone, siltstone||||||
10303|Legune Formation|65417|5|Briefly described|p158 Fig.2, p159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Correlated with the Pincombe Formation of the Carr Boyd Group (Halls Creek Orogen).||Topmost unit in Fitzmaurice Group.||Conformably overlies Lalngang Sandstone.||
10303|Legune Formation|69435|4|Described|p20:2-6|||Sweet et al. (1974). Fitzmaurice Basin. Exposed over a large area.||Fitzmaurice Group.||Conformably and gradationally overlies Lalngang Sandstone. Unconformably overlies Whitewater Volcanics.|Generally consists of monotonous medium-grained silica-cemented quartz sandstone / quartzite. Some beds can be traced up to 20km; others show lateral facies variations. Localised ferruginous phases are associated with groundwater movement.|12-JUL-16
10303|Legune Formation|69452|6|Mentioned|p36:10 Fig.36.7|Mesoproterozoic|Paleoproterozoic|Fitzmaurice Basin. Minimum age given as ?Mesoproterozoic.||||||12-JUL-16
10303|Legune Formation|69673|5|Briefly described|p59, p60 fig 48|||Up to 600m thick.||Fitzmaurice Group||Overlies Lalngang Sandstone|Silica cemented quartz sandstone or quartzite.|
10303|Legune Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, siltstone.|
10303|Legune Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10303|Legune Formation|73083|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||||
10340|Lennard Granite|23722|4|Described|p10|Proterozoic|Proterozoic|Intrudes Tarraji Microgranite. Geological Province: Hooper Complex||||||06-AUG-08
10340|Lennard Granite|24173|5|Briefly described|p7, p20|Paleoproterozoic|Paleoproterozoic|Age: c.1864Ma. Intrudes Marboo Formation||||||07-NOV-08
10340|Lennard 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
10340|Lennard Granite|30097|6|Mentioned|Table 27|||||||||
10340|Lennard Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10340|Lennard Granite|30526|6|Mentioned|p112|||||||||
10340|Lennard Granite|30533|4|Described|p14|||On Table 1||||||
10340|Lennard Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10340|Lennard Granite|30896|4|Described|p13|||Lower Proterozoic||||||
10340|Lennard Granite|30897|5|Briefly described|p9|||||||||
10340|Lennard Granite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10340|Lennard Granite|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10340|Lennard Granite|32660|5|Briefly described|Table 1|||||||||
10340|Lennard Granite|32728|6|Mentioned|Fig.3|||||||||
10340|Lennard Granite|33443|6|Mentioned|p261|||||||||
10340|Lennard Granite|36551|6|Mentioned|p45|||||||||
10340|Lennard Granite|36885|4|Described|p174|||||||||
10340|Lennard Granite|37462|4|Described|Table 4.I|||||||||
10340|Lennard Granite|37633|4|Described|Table 65|||See also P97.||||||
10340|Lennard Granite|38482|6|Mentioned|Table 1|||||||||
10340|Lennard Granite|41158|6|Mentioned|p19|||See also P149||||||
10340|Lennard Granite|41987|6|Mentioned|Fig.3 P73|||||||||
10340|Lennard Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
10340|Lennard Granite|42811|4|Described|p9|||||||||
10340|Lennard Granite|42814|5|Briefly described|p8|||||||||
10340|Lennard Granite|42815|5|Briefly described|map|||||||||
10340|Lennard Granite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
10340|Lennard Granite|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
10340|Lennard Granite|43819|6|Mentioned|p33|||||||||
10340|Lennard Granite|44155|4|Described|p234 Tb.3-2,p235 Fig.3-34,p240,p242-243|Paleoproterozoic|Paleoproterozoic|See also p246, p248 Tb.3-8. West Kimberley. Disrupted by WNW-trending Sandy Creek Shear Zone. Late to post-tectonic faulting: 1840 +/- 50 Ma. Appears as Lennard River Granite on p247.||Hooper Complex||Intrudes Whitewater Volcanics, Wombarella Quartz Gabbro. Is intruded by Kongorow Granite, Mount Amy Granite, Tarraji Microgranite. Equivalent to Chaneys Granite.|Grey porphyritic biotite granite; large tabular feldspar phenocrysts; locally non-porphyritic; local muscovite marginal phases.|
10340|Lennard Granite|48931|3|Fully described|p33|||||||||
10340|Lennard Granite|50437|5|Briefly described|p1.5, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1862 +/- 5Ma (SHRIMP).||||||06-NOV-15
10340|Lennard Granite|60533|5|Briefly described|p604|Paleoproterozoic|Paleoproterozoic|Age: 1862 +/- 5Ma (Griffin et al, 2000).||||||07-NOV-08
10340|Lennard Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1863 Ma|Paperbark Supersuite||||
10340|Lennard Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Age data from OZCHRON1. Comment: 'Reliable 207/206 age for the time of igneous crystallisation of this deformed part of the Lennard Granite, in excellent agreement with the 1864+/-4 Ma age for the undeformed body of the Lennard Granite.'|1862+/-5 Ma U/Pb SHRIMP|Paperbark Supersuite|Includes 2 unnamed sub-units.||foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite. Some zones rich in xenoliths of metasedimentary rocks.|
10340|Lennard Granite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Neoarchean||1862-2591 Ma|||||
10340|Lennard Granite|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.|1864-1862 Ma (isotopic)|Unit of Paperbark Supersuite.|||Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite|
10340|Lennard Granite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|1864 - 1862 Ma; Griffin et al. (2000).|Unit in Paperbark Supersuite.|||Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite.|
10340|Lennard Granite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|1864-1862 Ma (Griffin et al., 2000).|Paperbark Supersuite.|||Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite.|
10340|Lennard Granite|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv.|1862-1864 Ma|Paperbark Supersuite|||Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite.|
10340|Lennard 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, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files. Magmatic crystallisation age of 1867+\-6 Ma (weighted mean 207Pb/206Pb).|1864-1862 Ma (isotopic)|Unit of Paperbark Supersuite.||Intrudes into Mondooma Granite.|Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite, and equigranular metamonzogranite|
10340|Lennard Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|1864 - 1862 Ma.|Paperbark Supersuite.|||Foliated, coarse-grained, porphyritic biotite metamonzogranite; minor metasyenogranite, metagranodiorite and equigranular metamonzogranite.|
10340|Lennard Granite|72437|5|Briefly described|p62-64, p73-75, p77|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Porphyritic monzogranite.|
10343|Lennis Sandstone|22707|5|Briefly described|P15||Early Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|23571|5|Briefly described|p22|||See also Lennis Formation. Shallow marine shale and sandstone. Geological Province: Officer Basin||||||16-MAY-05
10343|Lennis Sandstone|23858|5|Briefly described|p919|Early Permian|Cambrian|Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|24067|5|Briefly described|p250|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|24161|4|Described|p9 Fig.6, p29|Devonian|Devonian|Unconformably overlies the Table Hill Volcanics. Unconformably overlain by the Wanna Formation. Geological Province: Gunbarrel Basin.||||||
10343|Lennis Sandstone|24390|5|Briefly described|p11 Fig. 6|Devonian|Silurian|Geological Province: Gunbarrel Basin.||||||
10343|Lennis Sandstone|31455|6|Mentioned|p12|||||||||
10343|Lennis Sandstone|31456|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31457|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31459|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31460|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31562|5|Briefly described|p9|||Refers Lennis et al. (1972)||||||
10343|Lennis Sandstone|31632|4|Described|Table 2|||See also p11.||||||06-SEP-18
10343|Lennis Sandstone|31633|4|Described|Table 2|||Mention p7.||||||06-SEP-18
10343|Lennis Sandstone|31634|4|Described|Table 1|||||||||
10343|Lennis Sandstone|31635|4|Described|Table 2|||||||||
10343|Lennis Sandstone|31636|5|Briefly described|p7|||See Table 2.||||||
10343|Lennis Sandstone|31638|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31639|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31640|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|31641|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31642|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|31914|2|Defined|p96|Carboniferous|Silurian|Ordovician to U.Carb.||||||
10343|Lennis Sandstone|32586|5|Briefly described|p114|||Refers Jackson (1966) p111.||||||06-SEP-18
10343|Lennis Sandstone|32648|6|Mentioned|p32|||Ludlovian||||||
10343|Lennis Sandstone|33586|4|Described|Table 1|||See also p12.||||||06-SEP-18
10343|Lennis Sandstone|33590|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|33591|5|Briefly described|p8|||||||||
10343|Lennis Sandstone|33592|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|33595|4|Described|Table 1|||||||||
10343|Lennis Sandstone|34417|6|Mentioned|p97|||||||||
10343|Lennis Sandstone|35123|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10343|Lennis Sandstone|36096|6|Mentioned|Fig.3|||||||||
10343|Lennis Sandstone|36257|6|Mentioned|Table 2.1|||||||||
10343|Lennis Sandstone|36701|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10343|Lennis Sandstone|36889|5|Briefly described|p219|||||||||
10343|Lennis Sandstone|36890|3|Fully described|p404|||||||||
10343|Lennis Sandstone|38329|6|Mentioned|p202|||||||||
10343|Lennis Sandstone|38898|6|Mentioned|Table 1|||||||||
10343|Lennis Sandstone|41276|6|Mentioned|p75|||||||||
10343|Lennis Sandstone|42030|5|Briefly described|p750|||||||||
10343|Lennis Sandstone|42734|5|Briefly described|map legend|Devonian||||||||
10343|Lennis Sandstone|44354|5|Briefly described|Map Legend||Early Permian|||||||
10343|Lennis Sandstone|45149|2|Defined|p39|Carboniferous|Silurian|Early Cambrian to Early Permian. See also Table 1 and Fig.12.||||||
10343|Lennis Sandstone|45168|6|Mentioned|Table 1|||See also p6.||||||
10343|Lennis Sandstone|46975|6|Mentioned|p86|||||||||
10343|Lennis Sandstone|49792|5|Briefly described|Fig.5|||||||||
10343|Lennis Sandstone|50085|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Age: <500Ma.  Geological Province: Officer Basin.||||||
10343|Lennis Sandstone|50205|5|Briefly described|p59 Fig.1,|Devonian|Devonian|Of Gunbarrel Basin.||||Is overlain unconformably by Wanna Formation.||
10343|Lennis Sandstone|61023|5|Briefly described|p15 Fig. 8|Ordovician|Ordovician|Geological Province: Gunbarrel Basin.||||||11-APR-08
10343|Lennis Sandstone|61272|6|Mentioned|p120 Fig.1|||See also Lennis Formation.||||||29-NOV-06
10343|Lennis Sandstone|62453|6|Mentioned|p6 Fig. 4, 22|||See also Lennis Formation? Overlies: Table Hill Volcanics.||||||
10343|Lennis Sandstone|64325|5|Briefly described|p82 Fig. 2|Middle Devonian|Early Devonian|Geological Province: Gunbarrel  Basin.||||||26-AUG-08
10343|Lennis Sandstone|64580|4|Described|map legend||Ordovician|Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone.||||||09-DEC-08
10343|Lennis Sandstone|64793|6|Mentioned|p286 Fig.5|Paleozoic|Paleozoic|||||||
10343|Lennis Sandstone|64970|6|Mentioned|p719, p719 Fig. 2, p720, p721 Fig. 6, 7|Devonian|Devonian|Geological Province: Officer Basin.||||||27-MAY-09
10343|Lennis Sandstone|65102|4|Described|p.366,370,373, 374, Figs4-41,4-49|Carboniferous|Late Devonian|Officer Basin. 50-425m; disconformable on Table Hill Volcanics, conformably overlain by Wanna Formation; red, fine to medium grained sandstone, commonly micaceous; micaceous siltstone interbeds; shallow marine but with some subaerial exposure; possibly also fluvial.||||||
10343|Lennis Sandstone|65363|6|Mentioned|p5 Fig.4, pp12-14, p19.|Ordovician|Ordovician|Shown repeatedly in this report as Lennis / Durba Sandstone, presumably for reasons of space. Southern Officer Basin. May correlate with Durba Sandstone in the northwest of the basin. Shown as Lennis Fm in Fig. 4, p5.||||Overlies Table Hill Volcanics. Is unconformably overlain by Paterson Formation.||
10343|Lennis Sandstone|65416|5|Briefly described|p137, p138 Fig.3, p139 Fig.4, pp144-146.|Early Carboniferous|Devonian|Officer Basin. Part of Sequence Pz4. Sandstone and claystone betweeen 100 and 465 m in Hussar 1, previously interpreted as Lennis Sandstone and Wanna Formation, are now included in Durba Sandstone. Age from fission-track analysis. Also called Lennis Formation on p145.||||Unconformably overlies Table Hill Volcanics and Browne Formation. Is overlain unconformably by Paterson Formation.||
10343|Lennis Sandstone|67195|5|Briefly described|p10 fig 6, p19 table 1,p40, p44, 47|Devonian|Devonian|Gunbarrel Basin. Probably misspelt as Lennis Formation in Fig 5 p9. Thermal conductivity of 2.60 W/mK. Basal unit of one well in this study. See also App 1, App 2.||||Unconformably overlain by Wanna Formation, Unconformably overlies Table Hill Volcanics|Partially friable, yellow medium grained sandstone.|
10343|Lennis Sandstone|67200|5|Briefly described|app 2 p8||||||||Partially friable medium grained sandstone.|
10343|Lennis Sandstone|69029|6|Mentioned|p329|Devonian|Devonian|Of Officer Basin.||||Overlain unconformably by Wanna Formation. Underlain unconformably by Table Hill Volcanics.||
10343|Lennis Sandstone|69091|5|Briefly described|p30 Fig.3.5, p37, see comments|Ordovician|Cambrian|Officer Basin. Misspelt as Lenis Sandstone on p44. Unconstrained as to age, but appears to be aeolian at least in part. See also p38 Fig.3.7, p41 Fig.3.8, p44, p81 Fig.4.17, p108 Fig.5.9, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||||Overlies Table Hill Volcanics; is overlain by Paterson Formation.||
10343|Lennis Sandstone|69153|6|Mentioned|500k_geologyp08_lut.csv||Ordovician||||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone|
10343|Lennis Sandstone|70634|4|Described|500k_geolgyp08_lut.csv|Ordovician|Ordovician||||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone.|
10343|Lennis Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Ordovician|Series 3|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|509-443.4 Ma (inferred)||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone; giant cross beds, possibly eolian|
10343|Lennis Sandstone|70826|6|Mentioned|p7 tbl 3|Ordovician|Cambrian|Officer Basin.||||||
10343|Lennis Sandstone|71146|5|Briefly described|p6, p26|Early Ordovician|Furongian|Officer Basin.||||Unconformably overlies the Table Hill Volcanics. Unconformably overlain by the Wanna Formation.|Sandstone.|
10343|Lennis Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
10343|Lennis Sandstone|71268|4|Described|GEOL_LUT_CSV files|Ordovician|Series 3|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|508-443.4 Ma (inferred)||||Fine- to medium-grained, feldspathic, micaceous sandstone; minor siltstone; giant cross-beds, possibly eolian|
10343|Lennis Sandstone|71618|6|Mentioned|p130|||Of Officer Basin.||||||
10343|Lennis Sandstone|71800|6|Mentioned|p26-p27|Middle Ordovician|Early Ordovician|Officer Basin.|||||Feldspathic sandstone.|
10343|Lennis Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Ordovician|Series 3|Officer Basin (Phase 2).|||||Fine- to medium-grained feldspathic micaceous sandstone, minor siltstone; giant cross beds, possibly eolian.|
10343|Lennis Sandstone|73346|6|Mentioned|p25|||Officer Basin.||||||
10352|Lerida 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
10352|Lerida Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
10352|Lerida Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10352|Lerida Granite|30533|5|Briefly described|p13|||On Table 1||||||
10352|Lerida Granite|32660|5|Briefly described|Table 1|||||||||
10352|Lerida Granite|36885|4|Described|p175|||||||||
10352|Lerida Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
10352|Lerida Granite|42811|5|Briefly described|p10|||||||||
10352|Lerida Granite|43281|5|Briefly described|Map legend||Proterozoic|||||||
10352|Lerida Granite|44155|4|Described|p242 Tb.3-5|||Compositionally similar to McSherrys Granodiorite.|1880 +/- 160 Ma.|Hooper Complex||Overlain by O'Donnell Formation.|Grey, porphyritic, biotite granite and granodiorite.|
10352|Lerida Granite|44366|14|Not recorded|p.8, Table 1||Proterozoic|Defintion on Tech.File E/52-5.||||||
10352|Lerida Granite|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971), part of Lamboo Complex.||||||
10352|Lerida Granite|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
10352|Lerida Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
10352|Lerida Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
10352|Lerida Granite|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 biotite granodiorite with green plagioclase and small mafic xenoliths|
10352|Lerida Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Foliated, porphyritic, biotite metagranodiorite; contains green plagioclase and small mafic inclusions.|
10352|Lerida Granite|72437|6|Mentioned|p64, p71, p73-74|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite||||
10360|Leveque Sandstone|7433|6|Mentioned|p44.|||||Unit in Broome Sandstone.||||
10360|Leveque Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10360|Leveque Sandstone|34363|6|Mentioned|p56|||Neocomian. See Fig.7.||||||
10360|Leveque Sandstone|36890|3|Fully described|p352|||||||||
10360|Leveque Sandstone|44997|14|Not recorded|p.25,26,27,38,50||Neocomian|||||||
10360|Leveque Sandstone|44998|2|Defined|p182, map|||Overlies Broome Sandstone. (E51-2/C.Leveque). See also App.6 p296.||||||
10360|Leveque Sandstone|45011|14|Not recorded|p64,71,72||Neocomian|||||||
10360|Leveque Sandstone|45153|2|Defined|App.8-135|Aptian|Aptian|Formerly Cape Leveque Sandstone.||||||
10363|Lewis Granite|22446|6|Mentioned|p20|Statherian|Statherian|||||||
10363|Lewis Granite|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Probably part of the Granites Supersuite. Geological province: Granites-Tanami Block. See also p82.||||||07-FEB-11
10363|Lewis Granite|29809|6|Mentioned|Table 1|||||||||
10363|Lewis Granite|29813|6|Mentioned|p7|||||||||
10363|Lewis Granite|35205|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10363|Lewis Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10363|Lewis Granite|36887|5|Briefly described|p206|||||||||
10363|Lewis Granite|38335|6|Mentioned|p1735|||||||||
10363|Lewis Granite|39559|6|Mentioned|Table 1|||||||||
10363|Lewis Granite|39888|6|Mentioned|Fig.8|||||||||
10363|Lewis Granite|41465|6|Mentioned|p13|||||||||
10363|Lewis Granite|42504|5|Briefly described|Table 3 P60|||||||||
10363|Lewis Granite|42754|6|Mentioned|p3|||||||||
10363|Lewis Granite|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
10363|Lewis Granite|44998|14|Not recorded|p.17|||||||||
10363|Lewis Granite|45140|1|Redefined|p12-13, p15-16, p22, p24-25, p32-35|Paleoproterozoic|Paleoproterozoic|See also p37-38, p47, p74, Appx.p10-11. Modified after Casey and Wells (1964). The Granites-Tanami Block. Named after Lewis Range. Previously included rocks now mapped as Slatey Creek Granite; now restricted to outcrops N and E of the Lewis Range (the original type locality) in the Lucas sheet area. A more precise type area is nominated in this study: a 40m high hill 1km WNW of Point Nelligan at 20 deg 11'30"S, 128 deg 38'00"E. Crops out mostly as gently sloping aprons of coarse granitic sand; also as tors, low rubbly mounds and flat-topped hills capped by laterite. Chemically, is essentially identical to Slatey Creek and The Granites Granites; geochemistry detailed.|1720+/-8 Ma (Rb-Sr whole-rock, Page et al. 1976).|||Intrudes the Killi Killi Beds (Tanami Complex). Is overlain by Gardiner and Lewis Range Sandstones.|Pinkish to pale grey muscovite or muscovite-biotite adamellite; local biotite adamellite and granodiorite. Cross-cutting sheets of pegmatite and aplite are common; local quartz veins, slickensides and fine-grained biotite-rich xenoliths.|
10363|Lewis Granite|46788|4|Described|p8|||||||||
10363|Lewis Granite|46864|6|Mentioned|p37|||Re age dates||||||
10363|Lewis Granite|48826|2|Defined|p.14||Paleoproterozoic|Tb.III, p.14,15,33,Pl.1. Granite of Lamboo Complex. Intrudes Halls Creek Metamorphics. Overlain by Phillipson Beds. ?L.Proterozoic. (E52-13,F52-2).||||||07-NOV-08
10363|Lewis Granite|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Granites-Tanami Block. Of the Granites Suite/Supersuite. Age: 1684 +/- 8Ma (Rb-Sr).||||||07-NOV-08
10363|Lewis Granite|62580|5|Briefly described|p47|||Of the Frederick Suite. Contains Orion Granodiorite (part of the composite Lewis Granite) analysed to show it consists of fine- to medium-grained, equigranular biotite granodiorite.||||||07-FEB-11
10363|Lewis Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
10363|Lewis Granite|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: 1795Ma. Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||10-MAY-21
10363|Lewis Granite|64580|4|Described|map legend||Paleoproterozoic|Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||09-DEC-08
10363|Lewis Granite|66129|5|Briefly described|p213, p214, p215 Fig.2, p216, p217|Statherian|Statherian|9000 sq. km, number of separate lobes. 1795 Ma. Monzogranite and granodiorite; medium to coarse grained quartz, white euhedral K-feldspar, plagioclase, primary muscovite, biotite. Accessory minerals: apatite, allanite, titanite, fluorite, pyrite, tourmaline, zircon.||||||
10363|Lewis Granite|66468|6|Mentioned|p17 Fig.3, p18 Fig.5, p20-21|Paleoproterozoic|Paleoproterozoic|See also p25-26 Figs.8,9; p27. Marked negative gravity anomalies and weakly magnetic.||||||
10363|Lewis Granite|68474|6|Mentioned|p573|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1795 Ma||||Monzogranite, granodiorite.|
10363|Lewis Granite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv; 500k_geologyp08_lut; and GEOCHRON. Granites-Tanami Complex. High gravity; non- to highly magnetic.|1792 +/- 5 Ma (Wingate et al., 2007).|Frederick Suite|||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite, diorite and/or gabbro.|
10363|Lewis Granite|69253|5|Briefly described|p759, p760-761 Figs.14-15, p762, p763|||Petrophysical properties described. Undergone ~6 km right-lateral displacement by Trans-Tanami Fault. See also p766, p767.||Unit in Frederick Suite.||Intrudes Dead Bullock Formation.||
10363|Lewis Granite|69426|6|Mentioned|p11:10, 11:12|||Blake et al. (1979).||Grimwade Suite.||||08-OCT-18
10363|Lewis Granite|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Sample GSWA 184802 (monzogranite) yielded a weighted mean 207Pb*/206Pb* date of 1792+\-5 Ma, interpreted as the age of magmatic crystallization of the monzogranite. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1815-1790 Ma (inferred)|Unit of Granites Supersuite.|||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite|
10363|Lewis Granite|70129|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1796 Ma (Bagas et al., 2010).||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. The two facies are mapped separately.|c.1796 Ma (Bagas et al., 2010).||||Muscovite and biotite monzogranite, locally porphyritic, minor biotite granodiorite; magnetite-bearing monzogranite.|
10363|Lewis Granite|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
10363|Lewis Granite|71080|6|Mentioned|p6|||At base of type section of Lewis Range Sandstone, 1.5 km southwest of Point Nelligan.||||Unconformably underlies Lewis Range Sandstone.||
10363|Lewis Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pegmatite, aplite, granodiorite, monzogranite|
10363|Lewis Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|1796+/-16 Ma.||||Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite. Magnetite-bearing monzogranite.|
10363|Lewis Granite|73089|4|Described|p3, p8-9, p13, p18-20, p38-39, p44|Orosirian|Orosirian|Granites-Tanami Orogen. A large composite body comprising magnetic and non-magnetic phases, which appears to reflect distinct magma batches emplaced during the same magmatic event. Assigned to the Frederick and Grimwade Suites. [See report for geochon details from six samples]. May be associated with the 1810-1790 Ma Stafford Event.|1807-1800 Ma|Frederick and Grimwade Suites||Intrudes Killi Killi Formation and Stubbins Formation.|Fine to medium grained monzogranites to granodiorites with rare mafic and fine-grained granitic xenoliths.|
10363|Lewis Granite|73445|5|Briefly described|p7|||Crowe and Muhling (1977). A corresponding biotite monzogranite in the Granites-Tanami Orogen has a U-Pb zircon age of 1825-1719 Ma.||||||
10365|Lewis Range Sandstone|22496|6|Mentioned|p9||Mesoproterozoic|Unconformably overlies the Gardiner Sandstone.||||||12-AUG-04
10365|Lewis Range Sandstone|23314|6|Mentioned|336|||||||||
10365|Lewis Range Sandstone|23621|5|Briefly described|p33|||Geological Province: Birrindudu Basin.||||||
10365|Lewis Range Sandstone|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Birrindudu Basin. Part of extensive sand blanket including Mount Kinahan Sandstone, Vaughan Springs Quartzite, Heavitree Quartzite and Townsend Quartzite||||||06-APR-05
10365|Lewis Range Sandstone|29813|4|Described|Table 2|||||||||
10365|Lewis Range Sandstone|29817|6|Mentioned|p10|||||||||
10365|Lewis Range Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10365|Lewis Range Sandstone|31360|6|Mentioned|Table 1|||||||||
10365|Lewis Range Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10365|Lewis Range Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10365|Lewis Range Sandstone|42504|5|Briefly described|Table 3 P60|||||||||
10365|Lewis Range Sandstone|45140|2|Defined|p13, p23-25, p40-41, p43, p46-48, p50-51|||See also p53, p55, p57, p75, Appx.p25-26. Crowe and Muhling (1977); Blake et al. (1977). Most of this unit was previously mapped as parts of Phillipson Beds and Kearney Beds (Well, 1962; Casey and Wells, 1964). Birrindudu Basin. Named after the Lewis Range: caps the NW-trending line of cuestas. 400m thick, up to 1000m. The type section is 1.5km SW of Point Nelligan, at 20deg 13'00"S, 128deg 38'00"E. Lateral equivalent of Munyu and Muriel Range Sandstones; ?correlated with Denison Beds. Mainly flat-lying or very gently dipping, except near faults.||Basal Redcliff Pound Group.||Unconformably overlies Killi Killi Beds, Gardiner Sandstone, Lewis and Slatey Creek Granites and ?Baines Beds. Is overlain conformably by Murraba Formation.|Friable, locally silicified, well-sorted, medium- to fine-grained quartz arenite; subordinate poorly-sorted sublithic arenite, quartz arenite, conglomerate and rare siltstone.|
10365|Lewis Range Sandstone|46788|6|Mentioned|p8|||||||||
10365|Lewis Range Sandstone|46864|4|Described|p38|||||||||
10365|Lewis Range Sandstone|62453|6|Mentioned|p16|||Geological Province: Murraba (formerly Birrindudu) Basin.||||||
10365|Lewis Range Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
10365|Lewis Range Sandstone|64277|5|Briefly described|Map ledgend|Neoproterozoic|Neoproterozoic|Of Redcliffe Pound Group. Geological Province: Murraba Basin, Centralian Superbasin. Cross-bedded quartz sandstone, ripple marks locally; minor sandstone, conglomerate, and siltstone.||||||24-JUN-08
10365|Lewis Range Sandstone|65074|4|Described|p351 fig 4-37, p353, p356 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of North/Centre Birrindudu Basin. 400 m (up to 1km) thick. Type section is 1.5 km SW of Point Nelligan in the Lewis Range.||Redcliff Pound Group||Overlain by Murraba Formation (conformably). Equivalent to Munyu Sandstone and Muriel Range Sandstone.|Quartz arenite, shale, siltstone, limestone, chert.|
10365|Lewis Range Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Neoproterozoic|Neoproterozoic|Murraba Basin. See also GEOCHRON.csv which gives two U-Pb zircon ages: 1021 +/- 33 Ma and 1067 +/- 20 Ma (both Blake et al., 2000).|1021 +/- 33 Ma (Pb/Pb).|Redcliff Pound Group||Unconformably overlies Slatey Creek Granite.|Cross-bedded quartz sandstone, with ripple marks, minor sandstone, conglomerate, and siltstone; chert, sublithic sandstone, siltstone, limestone; glauconitic sandstone, siltstone and shale, minor dolomitic sandstone.|
10365|Lewis Range Sandstone|68733|6|Mentioned|p188|Neoproterozoic|Neoproterozoic|Age shown as Neoproterozoic(?).||Redcliff Pound Group.||||05-DEC-17
10365|Lewis Range Sandstone|68994|6|Mentioned|p20|||Murraba Basin.||||Equivalent to Munyu Sandstone.||13-JAN-17
10365|Lewis Range Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Murraba Basin||Redcliff Pound Group|||Cross-bedded quartz sandstone, with ripple marks; minor sandstone, conglomerate, and siltstone.|31-JUL-15
10365|Lewis Range Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|Crops out in LUCAS and BILLILUNA map areas. Lithologically similar to Denison beds.||||Correlated with Munyu Sandstone and (probably) Denison beds.|Well-sorted, medium- to fine-grained quartz arenite, sublithic arenite, conglomerate and rare siltstone.|12-JUL-16
10365|Lewis Range Sandstone|69587|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Of Murraba Basin and Birrindudu Basin, Centralian Superbasin. Events: Alice Springs Orogeny. Sample GSWA 178851 (mature qtz-rich sandstone) yielded weighted mean 207Pb*/206Pb* dates of 1021+\-33 Ma, interpreted as maximum depositional age of the sandstone. Sample GSWA 178852 (qtz-rich sandstone) yielded weighted mean 207Pb*/206Pb* dates of 1067+\-20 Ma, interpreted as maximum depositional age of the sandstone. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.|830-810 Ma (inferred)|Unit of Redcliff Pound Group.||Basal unit of Redcliff Plain Group. Underlain unconformably by Slatey Creek Granite.|Cross-bedded quartz sandstone with ripple marks; glauconitic sandstone, conglomerate, siltstone, chert, limestone.|
10365|Lewis Range Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny.|830-810 Ma (Inferred)|Unit of Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate, and siltstone|
10365|Lewis Range Sandstone|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Is ovelain by Murraba Formation.|Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70141|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Overlies Birrindudu Group.|Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone. Separately mapped sub-units: chert, sublithic sandstone, siltstone and limestone; glauconitic sandstone, siltstone and shale, minor dolomitic sandstone.|
10365|Lewis Range Sandstone|70142|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.|Redcliff Pound Group.||Overlies Slatey Creek Granite.|Cross-bedded quartz sandstone, with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70143|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin. Unclear if age range refers to the Group or just the Lewis Range Sandstone.|830-810 Ma.|Redcliff Pound Group.|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate and siltstone.|
10365|Lewis Range Sandstone|70154|4|Described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic||810-1000 Ma|Redcliff Pound Group|||Cross-bedded quartz sandstone with ripple marks; minor sandstone, conglomerate, and siltstone|
10365|Lewis Range Sandstone|71080|4|Described|p8-11 23, 25-26, 27, 28, 29, 31, 32, 36|Tonian|Tonian|Basal unit, northern Murraba Basin. Type section discussed. Named for Lewis Range on LUCAS. Basal unit in the northern Murraba Basin. 20-400 m thick. Extent of unit in Kearney Range questioned. Previously included as the basal unit in the Redcliff Pound Group. Different detrital zircon spectra suggest younger age than Munyu Sandstone and/or different provenance. Part of the succession in the Kearney Range are more like Birrindudu Group rocks of the Birrindudu Basin and may be equivalnet to Hidden Basin beds. See also p4, 5, 6, 7,|detrital Zr max dep age 916 +/-43 Ma|||Unconformably overlies Lewis Granite at type section, Slatey Creek Granite. Previously considered a lateral equivalent of Munyu Sandstone, to Sth and Muriel Range Sandstone NT.|Dominated by well-sorted, fine- to medium grained, thin- to medium-bedded quartz arenite, with subordinate, poorly sorted, sublithic arenite, quartz arenite and conglomerate. Minor siltstone present locally.|04-FEB-19
10365|Lewis Range Sandstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1000-810 Ma (inferred)|Unit of Redcliff Pound Group.|||Cross bedded and rippled medium to fine grained quartz sandstone with shale pellet layers in places; minor shale, siltstone, limestone and chert with conglomerate and sublithic sandstone near the base|
10365|Lewis Range Sandstone|73086|6|Mentioned|p18, p30, p39|||Murraba Basin, southern.||||Potentially correlates to Bitter Springs Group.||
10365|Lewis Range Sandstone|73445|5|Briefly described|p7, 10, 12-14|||Whole-rock chemistry tabulated.||Redcliff Pound Group.||Is overlain by Murraba Formation. Equivalent to Munyu and Muriel Range Sandstones.|Fine-grained sandstone.|
10389|Liga Shale|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10389|Liga Shale|32660|5|Briefly described|Table 3|||||||||
10389|Liga Shale|32728|6|Mentioned|Table 5|||||||||
10389|Liga Shale|36551|6|Mentioned|Table 10|||||||||
10389|Liga Shale|36885|4|Described|p184|||||||||
10389|Liga Shale|44140|5|Briefly described|p294|Paleoproterozoic|Paleoproterozoic|45 m thick.||Crowhurst Group||Conformably overlies Hilfordy Formation. Is overlain conformably by Collett Siltstone.|Green fissile shale and micaceous siltstone.|07-MAR-18
10389|Liga Shale|44231|5|Briefly described|Map Legend||Proterozoic|Of the Crowhurst Group. Green shale; minor micaceous siltstone and silty sandstone.  Geological province: Crowhurst Basin.||||||19-MAY-05
10389|Liga Shale|44397|14|Not recorded|p.9,Table 2||Carpentarian|Crowhurst Group. Defn. on Tech.File E/52-9.||||||
10389|Liga Shale|44398|14|Not recorded|map legend||Carpentarian|||||||
10389|Liga Shale|45047|5|Briefly described|p28|||||||||
10389|Liga Shale|61574|5|Briefly described|p690|Proterozoic|Proterozoic|Of the Crowhurst Group.||||||
10389|Liga Shale|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Crowhurst Group.|||Green shale with minor interbeds of green micaceous siltstone and very fine micaceous silty sandstone|
10400|Lilian Formation|30388|4|Described|Table 1|||Middle Proterozoic age||||||
10400|Lilian Formation|30390|4|Described|p80|||See also P81||||||
10400|Lilian Formation|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mission Group||||||25-NOV-08
10400|Lilian Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10400|Lilian Formation|36551|6|Mentioned|Table 31|||||||||
10400|Lilian Formation|36886|4|Described|p198|||||||||
10400|Lilian Formation|67375|5|Briefly described|p38 Table 1, p51. |Mesoproterozoic|Mesoproterozoic|||Unit in Mission Group.||Overlies Frank Scott Formation. Is overlain by Milesia Formation.|Reddish to olive-green weathering shales.|
10400|Lilian Formation|67553|4|Described|p40,53-54|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Deposited in a deep water environment, however it is unknown is it was lacustrine or deep marine.||Unit of Mission Group.||Overlain by Milesia Formation. Underlain by Frank Scott Formation.|Reddish to olive-green weathering shales.|
10400|Lilian Formation|68995|5|Briefly described|p10, p19, p20|Stenian|Stenian|||Mission Group||Overlies the Frank Scott Formation.|Reddish to olive green weathering shales.|
10400|Lilian Formation|69091|6|Mentioned|p75|||Sedimentary lower part of Mission Group.||Mission Group|||Sedimentary.|
10400|Lilian Formation|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mission Group|||Shale, minor sandstone, limestone (including microbially laminated), dolomite, chert, microbialite, basalt, conglomerate, mudstone, metabasalt|
10400|Lilian Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mission Group.||Overlies Frank Scott Formation. Is overlain by Milesia Formation.|Shale; red to olive-green; minor sandstone, dolomite, chert, microbialite, basalt and conglomerate.|
10400|Lilian Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1040 Ma - 1057 Ma (Inferred)|Mission Group|||Shale; red to olive-green; minor sandstone, dolomite, chert, microbialite, basalt, and conglomerate|
10400|Lilian 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.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Shale; red to olive-green; minor sandstone, dolomite, chert, microbialite, basalt, and conglomerate|
10400|Lilian Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||ash tuff, basalt, chert, shale|
10400|Lilian 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, 1m_geologyp12_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Shale; red to olive-green; minor sandstone, dolomite, chert, microbialite, basalt, and conglomerate|
10403|Lillybooroora Conglomerate|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
10403|Lillybooroora Conglomerate|30897|4|Described|p18|||||||||
10403|Lillybooroora Conglomerate|30898|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
10403|Lillybooroora Conglomerate|38878|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
10403|Lillybooroora Conglomerate|41125|5|Briefly described|p42|||||||||
10403|Lillybooroora Conglomerate|42814|4|Described|p23|||||||||
10403|Lillybooroora Conglomerate|42815|5|Briefly described|map|Early Carboniferous|Late Devonian|||||||
10403|Lillybooroora Conglomerate|43281|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|||||||
10403|Lillybooroora Conglomerate|45158|3|Fully described|p22|||||||||
10403|Lillybooroora Conglomerate|64580|4|Described|map legend|Tournaisian|Famennian|Boulder and cobble conglomerate; minor sandstone and siltstone.||||||09-DEC-08
10403|Lillybooroora Conglomerate|66127|5|Briefly described|p384.|Carboniferous|Devonian||||||Conglomerate and sandstone.|
10403|Lillybooroora Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Famennian||||||Boulder and cobble conglomerate; minor sandstone and siltstone.|31-JUL-15
10403|Lillybooroora Conglomerate|69165|4|Described|500k_geologyp08_lut.csv||||||||Boulder and cobble conglomerate; minor sandstone and siltstone.|
10403|Lillybooroora Conglomerate|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Famennian||||||Boulder and cobble conglomerate; minor sandstone and siltstone|
10403|Lillybooroora Conglomerate|70154|5|Briefly described|500k_interpgeop14_lut.csv|Tournaisian|Upper Devonian||347-383 Ma||||Boulder and cobble conglomerate; minor sandstone and siltstone|
10403|Lillybooroora Conglomerate|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Canning Basin.||||||
10403|Lillybooroora Conglomerate|71267|4|Described|GEOL_LUT_CSV files|Tournaisian|Late Devonian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma); Red Bluffs Extension (372.2-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|382.7-350 Ma (inferred)||||Deltaic to alluvial fan conglomerate with pebbles, cobbles and boulders to 1.2m of quartzite derived from the King Leopold Sandstone, in a ferruginous sandstone matrix; overlain by rarely exposed sandstone|
10403|Lillybooroora Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Tournaisian|Late Devonian|Canning Basin.|||||Boulder and cobble conglomerate; minor sandstone and siltstone.|
10414|Limbunya Group|14019|4|Described|p4-6|Paleoproterozoic|Paleoproterozoic|Dolostone, siltstone, sandstone, tuffite. Unconformably overlies Inverway Metamorphics and Birrindudu Group; unconformably overlain by the Wattie Group. Max. thickness: 1300m. Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
10414|Limbunya Group|23314|5|Briefly described|329|||||||||
10414|Limbunya Group|23809|5|Briefly described|p47|Proterozoic|Proterozoic|Correlated with McArthur Group and possible with Namerinni Group (Tennant Inlier), and with Bungle Bungle Dolomite (Osmond Basin, W.A.). Geological Province: Birrindudu Basin.||||||30-MAR-05
10414|Limbunya Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24297|5|Briefly described|p4 Fig.3, p15|Proterozoic|Proterozoic|Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolomite, siltstone, sandstone, chert.||||||19-OCT-05
10414|Limbunya Group|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlies Birrindudu Group;  unconformably overlain by Wattie Group. Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|24442|5|Briefly described|p3, p50 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1640-1635Ma.  Geological Province: Victoria-Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|28255|3|Fully described|p10-11, Tb.11 (opp. p8)|||Now includes the former "Kirkimbie Beds". Subdivided into 11 formations. Extensive sequence of dolomite, siltstone and sandstone. Unconformably overlies Inverway metamorphics and Bunda Grit; unconformably overlain by the Wattie Group. Max. thick: >1300m.||||||22-DEC-08
10414|Limbunya Group|29804|6|Mentioned|p418|||||||||
10414|Limbunya Group|29805|4|Described|Table 1|||||||||
10414|Limbunya Group|29809|6|Mentioned|p418|||||||||
10414|Limbunya Group|30003|4|Described|p6, p9|||Predominantly dolomite, silty dolomite and siltstone, with subordinate sandstone and chert.  Age is Carpentarian or Adelaidean. Unconformably overlain by by the Wattie Group.||||||19-APR-05
10414|Limbunya Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
10414|Limbunya Group|31361|6|Mentioned|Table 1|||||||||
10414|Limbunya Group|32172|4|Described|p6|||Carpentarian or Adelaidean||||||
10414|Limbunya Group|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||16-NOV-04
10414|Limbunya Group|32175|5|Briefly described|Map legend|Adelaidean|Carpentarian|Dolomite, siltstone, sandstone, chert.||||||02-DEC-04
10414|Limbunya Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|32660|4|Described|Table 6|||||||||
10414|Limbunya Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Massive dark grey dolomite, chert.||||||02-DEC-04
10414|Limbunya Group|32701|4|Described|Table 1|||Adelaidean. See also p7.||||||30-OCT-06
10414|Limbunya Group|32728|6|Mentioned|p16|||||||||
10414|Limbunya Group|33374|6|Mentioned|p6|||Stratigraphy.||||||
10414|Limbunya Group|33375|4|Described|p7, p9 Tb. 1|||Carpentarian or Adelaidean.||||||26-APR-05
10414|Limbunya Group|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|33377|5|Briefly described|Table 2|||Strat.||||||
10414|Limbunya Group|33378|5|Briefly described|Map legend|||Age is Carpentarian or Adelaidean.||||||27-APR-05
10414|Limbunya Group|35950|6|Mentioned|p311|||||||||
10414|Limbunya Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10414|Limbunya Group|37462|4|Described|Table 4.V|||||||||
10414|Limbunya Group|38243|6|Mentioned|Fig.2|||||||||
10414|Limbunya Group|42504|6|Mentioned|p68|||Birrindudu Basin||||||
10414|Limbunya Group|45112|3|Fully described|p17|||p17-18||||||30-OCT-06
10414|Limbunya Group|45140|2|Defined|p12-13, p39-42, p53, p62, p74, Appx.p19|||Sweet et al. (1974). Birrindudu Basin. Named after Limbunya pastoral lease. Forms low strike ridges and undulating terrain. Over 400m thick. Folded about NW-trending axes. Mainly shallow-marine deposits.||||Unconformably overlies Bunda Grit and Inverway Metamorphics. Correlated with Birrindudu Group. Is overlain unconformably by Antrim Plateau Volcanics and Wattie Group.|Silicified medium- to fine-grained sublithic arenite and quartz arenite; cross-bedded, locally with ripple marks. Some beds contain shale pellets. Carbonate rocks.|
10414|Limbunya Group|46864|6|Mentioned|p38|||||||||
10414|Limbunya Group|48938|4|Described|p21|||Measured section p89.||||||30-OCT-06
10414|Limbunya Group|48943|2|Defined|p14|Adelaidean|Carpentarian|Carp. or Adel.||||||
10414|Limbunya Group|48950|3|Fully described|p38|||||||||
10414|Limbunya Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin.||||||07-FEB-11
10414|Limbunya Group|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Includes: Blue Hole Formation, Campbell Springs Dolostone, Fraynes Formation. Dolostone, siltstone, sandstone, tuffite.||||||07-NOV-08
10414|Limbunya Group|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes eleven named units and undivided rocks.  Consists of dolostone, siltstone, sandstone, tuffite.  Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Mainly dolostone, sandstone and siltstone. Geological Province: Birrindudu Basin.||||||07-NOV-08
10414|Limbunya Group|60682|5|Briefly described|piii, 7|Statherian|Statherian|Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|60685|5|Briefly described|p4 Fig. 3|Proterozoic|Proterozoic|Unconformably overlain by Wickham Formation (Wattie Group). Geological Province: Birrindudu Basin.||||||
10414|Limbunya Group|63261|5|Briefly described|p17, p24|Paleoproterozoic|Paleoproterozoic|Interpreted to overlie Birrindudu Group to the north (drill hole evidence). Age: 1640-1635Ma (SHRIMP U-Pb, tuffaceous rock, Smith et al 2001).|Age: 1640-1635Ma|||||07-FEB-11
10414|Limbunya Group|64662|5|Briefly described|p44|Statherian|Statherian|Age: ~1.64Ga. Overlies Birrindudu Group in the Victoria River Basin.||||||07-FEB-11
10414|Limbunya Group|64722|5|Briefly described|Fig. 2 p3-6, p10|Statherian|Statherian|Age of 1640-1635 Ma given after Cutovinos et al. (2002).||||Overlies Birrindudu Group.||11-APR-12
10414|Limbunya Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Victoria River and Birrindudu Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
10414|Limbunya Group|64737|4|Described|p232 Fig.2, p233, p243|Statherian|Statherian|Of Victoria River Basin. Ages from volcanics within the unit (Cutovinos et al., 2002).|1636 +/- 5 and 1639 +/- 7 Ma.||Includes Bluehole Formation and Campbell Springs Dolostone.|Overlies Gardiner Sandstone.|Interlayered siliciclastic and hypersaline carbonate rocks which include stromatolites and other features interpreted as shallow to very shallow marine deposition.|30-APR-12
10414|Limbunya Group|65074|6|Mentioned|p349, p351 fig 4-37, p352|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||||
10414|Limbunya Group|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Birrindudu Basin. Includes Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation. Dolostone, siltstone, sandstone, tuffite||||||
10414|Limbunya Group|65342|5|Briefly described|pp10-11.|||Birrindudu Basin.|||Includes Stirling, Kunja and Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Fraynes and Killaloc Formations; Pear Tree, Mallabah and Campbell Springs Dolostones.|Unconformably overlies Birrindudu and Tolmer Groups.|Mainly carbonate and siliciclastic rocks.|
10414|Limbunya Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Stirling and Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Killaloc and Fraynes Formations; Pear Tree, Mallabah and Campbell Springs Dolostones; and Kunja Siltstone.|Is unconformably overlain by Wattie Group.||
10414|Limbunya Group|67269|6|Mentioned|p20-21 Fig.19|||Birrindudu Basin.|||Pear Tree Dolomite.|||
10414|Limbunya Group|68280|6|Mentioned|p26 fig 24|||Birrindudu Basin.|||Includes Pear Tree Dolomite|||
10414|Limbunya Group|68733|4|Described|p176-179, p181, p184-187, p193|Statherian|Statherian|Birrindudu Basin. Age constraints provided by four intercalated tuffs in the upper parts (Smith 2001; Cutovinos et al. 2002). No longer marks the subdivision between Birrindudu and Victoria Basins; replaced by top-Tijunna Group unconformity. Uncertain correlation with Birrindudu Group discussed.|ca. 1640 - 1635 Ma||Includes Killaloc, Fraynes, Blue Hole, Amos Knob and Margery Formations; Campbell Springs, Pear Tree, and Mallabah Dolostones; Faraquharson Sandstone and Stirling (basal) Sandstones; Kunja Siltstone.|Unconformably overlain by the Wickham Formation.  Unconformably underlain by the Birrindudu Group.|Carbonate dominated.|05-DEC-17
10414|Limbunya Group|69417|5|Briefly described|p2:5-6|Statherian|Statherian|Southern Birrindudu Basin.|c.1650-1630 Ma.|||||12-JUL-16
10414|Limbunya Group|69425|6|Mentioned|p10:4|||Mentioned as possible correlative of Hatches Creek Group, based on geochronological grounds.||||||12-JUL-16
10414|Limbunya Group|69429|5|Briefly described|p14:2|Paleoproterozoic|Paleoproterozoic||||Stirling, Farquharson Sandstones; Margery, Amos Knob, Blue Hole Formations; Pear Tree, Mallabah, Campbell Springs Dolostones; Kunja Siltstone.|Unconformably overlies Inverway Metamorphics.||12-JUL-16
10414|Limbunya Group|69430|5|Briefly described|p15:19|Statherian|Statherian|Birrindudu Basin. Has tuffaceous units with similar ages to tuffaceous units dated at 1639 +/- 3 Ma in the HYC Pyritic Shale Member of the Barney Creek Formation (McArthur Group), McArthur Basin.||||||12-JUL-16
10414|Limbunya Group|69432|4|Described|p17:1-3, 5-9, 12-13|Paleoproterozoic|Paleoproterozoic|Assigned to the Birrindudu Basin by Dunster et al. (2000). Previously assigned to the Victoria Basin. Composite thickness of c.1300m. Generally dips at very low angles; has locally developed broad gentle folds. Exploration target for base metals.|||Stirling, Farquharson Sandstones; Margery, Amos Knob, Blue Hole, Fraynes, Killaloc Formations; Mallabah, Pear Tree, Campbell Springs Dolostones.|Unconformably overlies Birrindudu and Tolmer Groups. Is overlain unconformably by Wattie Group.|A succession of cyclic carbonate and siliciclastic rocks. Minor subaqueous tuffaceous beds.|12-JUL-16
10414|Limbunya Group|69435|5|Briefly described|p20:1|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Possible correlative of the Fitzmaurice Group.|c.1640 Ma.||||Predominantly carbonates and evaporites.|12-JUL-16
10414|Limbunya Group|69448|5|Briefly described|p33:8|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Stirling Sandstone.|||12-JUL-16
10414|Limbunya Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p188|Statherian|Statherian|Approximately 1300m thick. Age ranging from 1830-1638 Ma. Also includes the Kunja Siltstone, Farquharson Sandstone, Blue Hole Formation, Campbell Springs Dolostone, Fraynes Formation, Killaloc Formation.|||Includes Stirling Sandstone, Margery Formation, Pear Tree Dolostone, Amos Knob Formation, Mallabah Dolostone|Unconformably overlies Birrindudu Group, unconformably overlain by Wattie Group|Dolostone and dolomitic siliciclastic rocks.|
10414|Limbunya Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].|||Includes Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation.|||18-JUL-16
10414|Limbunya Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Fraynes, Killaloc, Blue Hole, Amos Knob, Margery Formations, Campbell Springs, Mallabah Dolostones, Farquharson Sandstone, Kunja Siltstone,  Pear Tree Dolostone, Stirling Sandstone.|Is unconformably overlain by Wattie Group.||
10414|Limbunya Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Stirling Sandstone, Margery Formation.|||
10414|Limbunya Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Pear Tree, Mallabah, Campbell Springs Dolostones; Amos Knob, Blue Hole, Fraynes Formations; Kunja Siltstone; Farquharson Sandstone.|Is overlain unconformably by Wattie Group.|Dolostone, siltstone, sandstone, shale, chert.|
10414|Limbunya Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. No outcrop in map area: shown in Section only.|||Fraynes, Killaloc Formations.|Is overlain unconformably by Wickham Formation (Wattie Group).|Dolostone, siltstone, sandstone, chert.|
10414|Limbunya Group|70968|6|Mentioned|p6|||Birrindudu Basin.||||Is overlain unconformably by Roper Group.||
10414|Limbunya Group|71169|5|Briefly described|p71|Statherian|Statherian|North Australian Craton.|c. 1650 Ma|||||
10414|Limbunya Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, siltstone|
10414|Limbunya Group|71302|5|Briefly described|p2-3,6,72-74|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Also includes Amos Knob Formation, Pear Tree Dolostone, Margery Formation, Stirling Sandstone.|||Includes Killaloc Formation, Fraynes Formation, Campbell Springs Dolostone, Blue Hole Formation, Farquharson Sandstone, Kunja Siltstone, Mallabah Dolostone.|Overlain by Wattie Group. Underlain by Birrindudu Group or Tolmer Group.||
10414|Limbunya Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p36|Mesoproterozoic|Palaeoproterozoic|Birrindudu Basin.|||Includes the Farquharson Sandstone.|||
10414|Limbunya Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Basin. Broadley equivalent to Glyde package, and Habgood, Balma, McArthur and Vizard groups (McArthur Basin).||||||
10414|Limbunya Group|73083|6|Mentioned|p30-31|||[Also written as Limbunya group].||||Unconformably overlain by Wickham Formation (Wattie Group).||
10424|Limmen Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
10424|Limmen Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10424|Limmen Sandstone|22853|3|Fully described|26|Proterozoic|Proterozoic|Of the Roper Group. Max thickness 80m. Overlain by Mainoru Formation, underlain by McArthur Group and Nathan Group.||||||30-OCT-06
10424|Limmen Sandstone|23216|5|Briefly described|p30,33-4|||||||||
10424|Limmen Sandstone|23404|5|Briefly described|p639 Fig.2|||Of Roper Group.||||||
10424|Limmen Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Roper Group||||||
10424|Limmen Sandstone|23937|2|Defined|p83 App. 1|Calymmian|Calymmian|Of Collara Subgroup. Previously mapped as Mallison Sst and lower Wigram Fm of Malay Road Group. Conformably overlain by Gibb Mbr; overlies Mantungula Fm with erosive contact.  Thickness in Roper area: 100m: 330m In TANUMBIRINI. Geol.Prov: McArthur Basin.||||||01-NOV-04
10424|Limmen Sandstone|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
10424|Limmen Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Does not crop out in BLUE MUD BAY map sheet. Subdivided into two units: first, quartz arenite, and second, upper part: sandstone with lower part: mudstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
10424|Limmen Sandstone|24050|3|Fully described|p41, P9 Tb. 2|Mesoproterozoic|Mesoproterozoic|Of Roper Group.  Granule- and pebble-rich quartz sandstone overlain by fine- to medium-grained quartz sandstone.  Overlies Dook Creek Formation; underlies Mainoru Formation.  Max. thickness: 60m.||||||30-OCT-06
10424|Limmen Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||23-DEC-09
10424|Limmen Sandstone|24303|5|Briefly described|p60 Appendix|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: McArthur Basin. Correlative of upper part of Sweetwater Member (Baralandji Formation). See also p24 Tb.4.||||||
10424|Limmen Sandstone|32660|5|Briefly described|Table 4|||||||||
10424|Limmen Sandstone|39210|6|Mentioned|p51|||||||||
10424|Limmen Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10424|Limmen Sandstone|40691|6|Mentioned|p64|||Mention Fig.4||||||
10424|Limmen Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10424|Limmen Sandstone|41220|6|Mentioned|Fig.3|||||||||
10424|Limmen Sandstone|41268|5|Briefly described|Fig.4|||Mention p290.||||||30-OCT-06
10424|Limmen Sandstone|41531|6|Mentioned|p167|||||||||
10424|Limmen Sandstone|42385|4|Described|p26|||See also Table 5 p25.||||||30-OCT-06
10424|Limmen Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
10424|Limmen Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
10424|Limmen Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Lower Roper Group (Roper Group).||In schematic section, underlies Mainoru Formation; overlies Mantungula Formation.|Ridge forming: structureless quartzarenite interbedded with micaceous siltstone; sandstone, pebbly sandstone; basal regolith structure. Detailed lithology given.|25-AUG-14
10424|Limmen Sandstone|42639|4|Described|p38|||||||||
10424|Limmen Sandstone|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
10424|Limmen Sandstone|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Predominantly fine to medium grained, thin to medium bedded quartzarenite with thin interbeds of micaceous mudstone.||||||19-OCT-05
10424|Limmen Sandstone|42812|3|Fully described|p45, Table 5|||Of Roper Group.||||||30-OCT-06
10424|Limmen Sandstone|42846|5|Briefly described|p503, Fig.1 p502|||Basal unit of Roper Group.||||||09-MAY-05
10424|Limmen Sandstone|43010|6|Mentioned|p145|||||||||
10424|Limmen Sandstone|43036|4|Described|p57|||Of Roper Group.||||||30-OCT-06
10424|Limmen Sandstone|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||30-OCT-06
10424|Limmen Sandstone|43652|6|Mentioned|p386|||||||||
10424|Limmen Sandstone|44112|3|Fully described|Table12p68,69|||||||||
10424|Limmen Sandstone|44287|14|Not recorded|p.12, opp.11|||(E53-3).||||||
10424|Limmen Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, sandstone, siltstone Conglomerate. Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
10424|Limmen Sandstone|44300|14|Not recorded|map legend|||SD/53-7,8. Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44332|14|Not recorded|p.7,opp.6,map|||(D53-14).||||||
10424|Limmen Sandstone|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
10424|Limmen Sandstone|44400|2|Defined|p.9,12,Tb.1,opp.p.6|||Mt. Marumba (D53-6), map.||||||
10424|Limmen Sandstone|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44434|14|Not recorded|p.7,8, opp.p.6, map|||||||||
10424|Limmen Sandstone|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44436|5|Briefly described|p.10-13,opp. p.7,map|||(E53-4).||||||02-DEC-04
10424|Limmen Sandstone|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Massive fine- to medium-grained quartz sandstone, micaceous siltstone.  Conformably overlies the Karns Dolomite; conformably overlain by Mainoru Formation. Upper (?) Proterozoic.||||||08-DEC-04
10424|Limmen Sandstone|44459|14|Not recorded|p.8,9,opp.p.6, map|||(E53-2).||||||
10424|Limmen Sandstone|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44471|14|Not recorded|p.9, opp.p.7, map|||(D53-10).||||||
10424|Limmen Sandstone|44472|5|Briefly described|map legend|||Of the Roper Group.  Massive and flaggy silicified quartz sandstone,micaceous quartz greywacke; basal quartz pebble conglomerate.  Upper (?) Proterozoic.||||||02-DEC-04
10424|Limmen Sandstone|44473|14|Not recorded|p.10, opp. p.7|||(E53-7). Basal Formation of Roper Group.||||||
10424|Limmen Sandstone|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|44530|14|Not recorded|p.11,14, opp.12|||(D53-15).||||||
10424|Limmen Sandstone|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
10424|Limmen Sandstone|45022|5|Briefly described|p.80||Adelaidean|Of Roper Group. Tb.11. Pl.28.||||||
10424|Limmen Sandstone|45162|4|Described|p151, p4 Fig.4, p105|Proterozoic|Proterozoic|||Of Roper Group||||26-MAR-18
10424|Limmen Sandstone|46861|6|Mentioned|Fig.2|||||||||
10424|Limmen Sandstone|60483|5|Briefly described|p7 Fig. 5, p32|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
10424|Limmen Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Mainoru Formation, underlain by Mantungula Formation.||||||
10424|Limmen Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Quartz sandstone: thick to very thick bedded, fine-to coarse-grained, graniule to pebble-rich towards base; minor micaceous siltstone. Overlies Mantungula Formation; underlies Mainoru Formation.||||||15-FEB-05
10424|Limmen Sandstone|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlies the Mantungula Formation. Overlain by the Mainoru Formation. Pink to white fine-grained quartzose sandstone with current lineation.||||||
10424|Limmen Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Quartz sandstone: thick to very thick bedded, fine to very coarse grained, granule to pebble rich towards base, planar and trough cross bedded, current ripples; minor micaceous siltstone.||||||
10424|Limmen Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Does not crop out in BLUE MUD BAY map sheet. Subdivided into two units: first, quartz arenite, and second, upper part: sandstone with lower part: mudstone. Geol. Prov: McArthur Basin.||||||
10424|Limmen Sandstone|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Oldest unit of the Roper Group. Morphologically prominent mature quartzite and sandstone deposits; exhibits shatter cones related to the Strangways impact event, and occasionally monomict brecciation. Geological Province: McArthur Basin.||||||26-APR-06
10424|Limmen Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
10424|Limmen Sandstone|64784|5|Briefly described|p2 Fig.2 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|64815|6|Mentioned|p5 Fig.3, p17  |||||Of the Roper Group.||||
10424|Limmen Sandstone|64816|6|Mentioned|p2 Fig.1 |||||Unit in Roper Group.||||
10424|Limmen Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
10424|Limmen Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
10424|Limmen Sandstone|65228|5|Briefly described|Figs.02, 24.|||McArthur Basin.||Unit in Roper Group.||Overlies Mantungula Formation and Dungaminnie Formation. Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
10424|Limmen Sandstone|65340|4|Described|p62, pp66-67. |Mesoproterozoic|Mesoproterozoic|Forms a broad north-striking resistant ridge in western ROBINSON RIVER. Outcrops as large, rounded boulders. Occasional planar and trough crossbeds; rare asymmetric ripples. Interpreted as marine shelf deposits, above fair-weather wave base. Forms a concentrically striking outcrop around a 6 km diameter circular outcrop of Bukalara Sandstone at the Foelsche impact structure.||Unit in Roper Group.||Overlies Mantungula Formation; locally unconformably overlies Karns Dolomite. Is overlain by Mainoru Formation.|White to pale pink or maroon, strongly silicified, medium to thickly bedded, fine quartzose sandstone; characteristic fine parallel lamination; poorly bedded to massive; thin brown iron oxide weathered carapace.|
10424|Limmen Sandstone|65342|6|Mentioned|p8.|||McArthur Basin. Max. thickness at least 39 m.||Unit in Roper Group.||Overlies Mantungula Formation. Is overlain by Mainoru Formation.||
10424|Limmen Sandstone|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Ridge-forming.||Unit in Roper Group.||Overlies Balbirini Dolostone. Is overlain by Mainoru Formation.|Fine-grained structureless quartz arenite with clay clast imprints, minor ripples and cross-beds; interbedded with grey micaceous siltstone; very fine-grained sandstone and iron-stained, poorly-sorted pebbly sandstone; local basal regolith breccia.|
10424|Limmen Sandstone|67352|4|Described|p13 Tb.2, p58|Calymmian|Calymmian|McArthur Basin. 1350m thick.||Roper Group||Overlies (unconformably) Nathan or McArthur Groups. Overlain conformably by Mainoru Formation.|Fine- to medium-grained quartz arenite, commonly equant and intensely silicified; local tabular micaceous or pebbly sandstone, siltstone, limestone; basal beds conglomeratic or silty.|
10424|Limmen Sandstone|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
10424|Limmen Sandstone|69430|4|Described|p15:3, 24-27, 30, 34, 43, 48, 62|Calymmian|Calymmian|McArthur Basin. 20-100m thick. Fluvial to shallow-marine shoreline sandstone.||Basal Collara Subgroup.||Overlies Dook Creek Formation (Mount Rigg Group) unconformably and Mantungula Formation ?disconformably (erosive contact). Is overlain conformably by Gibb Member (Mainoru Formation).|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|12-JUL-16
10424|Limmen Sandstone|69673|6|Mentioned|p16 fig 13|||McArthur Basin.||Collara Subgroup||Overlain by Mainoru Formation, Unconformably? Overlies Dook Creek Formation||
10424|Limmen Sandstone|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Tidal platform sandstone.||Of Collara Subgroup.||Overlies Mantungula Formation, overlain by Mainoru Formation.||
10424|Limmen Sandstone|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Mantungula Formation; overlain by Gibb Member (Mainoru Formation).|Sandstone.|
10424|Limmen Sandstone|70897|5|Briefly described|p43, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Roper Group.||Overlies Dungaminnie Formation unconformably and Mantungula Formation conformably.|Fine- to medium-grained quartz sandstone; commonly with pebbles of chertified carbonates at the base.|
10424|Limmen Sandstone|70968|2|Defined|p6, p10-17, p21-23, p25, p124, p126-129|Calymmian|Calymmian|See also p131, p138-140, p143-144. Sweet in Abbott et al. (2001) after Dunn (1963). Originally mapped as Canopy Rock Sandstone (Ruker, 1959); also mapped as Mallison Sandstone and lower Wigram Formation of the Malay Road Group, and as part of Baralminar beds: all these names are superseded. Previously included rocks now part of Mantungula Formation; and the upper part near Roper Bar has been reassigned to the Gibb and Wadjeli Sandstone Members of Mainoru Formation. Named after Limmen Bight River. Type section is near Mission Gorge, from 477100mE 8378900mN (base) to 478100mE 8381000mN in URAPUNGA sheet. Forms mesas, cuestas or narrow ridges. Very widespread. Represents basal Roper Group locally. Lithology described and illustrated in detail. Shallow marine deposits. Thickness c.130m to estimated maximum of c.300m. Detrital zircon diagram.||Collara Subgroup.||Overlies Mantungula Formation conformably; Dook Creek Formation (Mount Rigg Group), McArthur and Nathan Groups unconformably; Urapunga Granite nonconformably. Conformably underlies Mainoru Formation.|Indurated, white, thickly bedded, medium- to very coarse-grained quartz sandstone, minor pebbly sandstone and conglomerate; overlain by fine- to medium-grained, well sorted quartz sandstone with thin interbeds of micaceous sandstone and siltstone.|
10424|Limmen Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 15 - 130+ m thick. Coastal tidal platform, possibly some fluvial, deposits.||Collara Subgroup.||Conformably overlies Mantungula Formation. Is overlain conformably by Gibb Member, and locally disconformably by Nullawun Member, (Mainoru Formation).|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|
10424|Limmen Sandstone|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Mantungula Formation. Overlain by the Mainoru Formation.||
10424|Limmen Sandstone|71494|4|Described|p2-p4, p7-p8, p17-p19, p22-p23, p26|||20-100m thick. Deposited in a fluvial to shallow marine or shoreline environment. Referred to as the Limmen Formation on p23.||||Unconformably overlies the Mantungula Formation. Conformably overlain by the Gibb member; disconformably overlain by the Nullawun Member.|Fine to very coarse and granule-rich quartz sandstone; minor micaceous siltstone.|
10424|Limmen Sandstone|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
10424|Limmen Sandstone|71893|3|Fully described|iii, p2-p5, p8, p13-p15|Calymmian|Calymmian|McArthur Basin. A type section occurs near Mission Gorge in the Collara Mountains about 10km northeast of Ngukurr in central-northern Urapunga. Zircon description, description at type section, sample locality, LAICPMS U-Pb and Hf analysis, results and interpretation are provided. The youngest individual date obtained was 1615 +/- 50 Ma a maximum depositional age of 1629 +/- 23 Ma was obtained. 5-10m thick. Age is constrained to be between 1589 +/- 3 Ma to 1492 +/- 4 Ma on the basis of dating of the underlying Nathan Group and overlying Showell Member respectively.||Collara Subgroup||Disconformably (probably) overlies the Mantungula Formation. Unconformably overlies the McArthur and Nathan groups. Conformably (locally disconformably) overlain by the Mainoru Formation.|Thickly- to very thickly-bedded, medium- to very coarse-grained or granule rich fluvial quartz sandstone overlain by a medium to thickly bedded, fine-grained quartz sandstone.|
10424|Limmen Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Minimum age from overlying Mainoru Formation.||Collara Subgroup||Overlies Mantungula Formation and underlies Mainoru Formation.||
10424|Limmen Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Collara Subgroup, Roper Group||Partly underlain by Mantungula Formation. Overlain by Mainoru Formation.||
10424|Limmen Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Collara Subgroup||Overlies Mantungula Formation and underlies Mainoru Formation.||
10424|Limmen Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Mantungula Formation. Overlain by Mainoru Formation.||
10424|Limmen Sandstone|73083|6|Mentioned|p40|||||||||
10424|Limmen Sandstone|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Mantungula Formation. Overlain by Gibb Member, Mainoru Formation.|Includes tidal Sandstone.|
10424|Limmen Sandstone|73280|6|Mentioned|p1, p4-5, App.1A, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
10424|Limmen Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Collara Subgroup.||Unconformably overlies upper Balbirini Dolostone (Nathan Group). Is overlain by Mainoru Formation.||
10441|Linnekar Limestone|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Geological Province: Ord Basin.||||||
10441|Linnekar Limestone|22537|5|Briefly described|40|||||||||
10441|Linnekar Limestone|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.  Maximum thickness: 40m.||||||
10441|Linnekar Limestone|24303|6|Mentioned|p63 Appendix|||Geological Province: Ord Basin. Correlative of Gum Ridge Formation.||||||
10441|Linnekar Limestone|28255|3|Fully described|p97, Tb. 9 (before p83), p144 App.|Late Cambrian|Cambrian|Of the Negri Group. Grey, flaggy, crystalline limestone with interbedded siltstone and shale; chert nodules abundant; fossiliferous. Conformably overlies Nelson Shale; conformably underlies Panton Formation. Max. thickness: 20m. Geol.Prov: Hardman Basin.||||||03-DEC-12
10441|Linnekar Limestone|32172|4|Described|Table 2|||Middle Cambrian. Negri Gp.||||||
10441|Linnekar Limestone|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Grey, flaggy, fossiliferous limestone, minor siltstone interbeds.  Conformably underlies the Panton Formation; conformably overlies the Nelson Shale.||||||17-NOV-04
10441|Linnekar Limestone|32648|6|Mentioned|p32|||M. Camb.||||||
10441|Linnekar Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
10441|Linnekar Limestone|36551|6|Mentioned|Table 16|||||||||
10441|Linnekar Limestone|36890|3|Fully described|p397|||||||||
10441|Linnekar Limestone|39210|6|Mentioned|p48|||||||||
10441|Linnekar Limestone|40993|6|Mentioned|Fig.1|||||||||
10441|Linnekar Limestone|40996|6|Mentioned|p403|||||||||
10441|Linnekar Limestone|41840|3|Fully described|p42|||||||||
10441|Linnekar Limestone|41864|4|Described|p18|||||||||
10441|Linnekar Limestone|41865|5|Briefly described|Map legend||Early Cambrian|||||||
10441|Linnekar Limestone|41866|5|Briefly described|Map legend|Early Cambrian||||||||
10441|Linnekar Limestone|42070|6|Mentioned|Fig.9 P12|||||||||
10441|Linnekar Limestone|42477|5|Briefly described|p68|||||||||
10441|Linnekar Limestone|42771|6|Mentioned|p15|||||||||
10441|Linnekar Limestone|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
10441|Linnekar Limestone|44317|4|Described|Table 4||Cambrian|||||||
10441|Linnekar Limestone|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian.||||||
10441|Linnekar Limestone|44363|5|Briefly described|p.6,18,21||Middle Cambrian|Middle Cambrian (Negri Group).||||||
10441|Linnekar Limestone|44364|14|Not recorded|map legend|||||||||
10441|Linnekar Limestone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
10441|Linnekar Limestone|44965|14|Not recorded|Not recorded|||||||||
10441|Linnekar Limestone|45055|6|Mentioned|p10|||Fossil locality||||||
10441|Linnekar Limestone|45062|6|Mentioned|p74|||||||||
10441|Linnekar Limestone|48943|3|Fully described|p109|||Strat. table p140.||||||30-OCT-06
10441|Linnekar Limestone|60419|3|Fully described|p1, 3 Fig.2, p6-7|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Nelson Shale. Conformably overlain by Panton Formation. Max. thickness: 40m. Thinly bedded calcimudstone, marl and mudstone, and thicker bioclast wackestone. Contains Ordian fauna. Geological Province: Ord Basin.||||||
10441|Linnekar Limestone|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Laminated micritic limestone, shale and calcareous shale; contains chert, stromatolites, and macrofossils locally. Geological Province: Ord Basin.||||||03-NOV-04
10441|Linnekar Limestone|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Stromatolitic and fossiliferous limestone and calcareous shale, local chert. Conformably overlies the Nelson Shale; conformably overlain by Panton Formation.  Geological Province: Ord Basin.||||||15-DEC-08
10441|Linnekar Limestone|62789|6|Mentioned|p133|Cambrian|Cambrian|In Ord Basin. Contains Redlichia forresti assemblage of very low diversity.||||||
10441|Linnekar Limestone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
10441|Linnekar Limestone|67352|6|Mentioned|p20|Middle Cambrian|Middle Cambrian|Ord Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
10441|Linnekar Limestone|67860|4|Described|p417 fig 4-85, p419 Tb. 4-18, p421|Middle Cambrian|Middle Cambrian|8-24 m thick. Type section details given. Fossiliferous.||Negri Subgroup||Conformably overlies Nelson Shale. Is overlain conformably by Panton Formation.|Basal micritic limestone with chert nodules; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3||Ord Basin||Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|31-JUL-15
10441|Linnekar Limestone|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Nelson Shale. Is overlain by Panton Formation.||12-JUL-16
10441|Linnekar Limestone|69446|6|Mentioned|p31:3|||Ord Basin. Strong species-level similarity with correlative faunas of Tindall Limestone (Daly Basin).||||||12-JUL-16
10441|Linnekar Limestone|69447|6|Mentioned|p32:2|||Ord Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
10441|Linnekar Limestone|69448|4|Described|p33:2-6, 8|Middle Cambrian|Middle Cambrian|Traves (1955); Playford et al. (1975). Ord Basin. Up to 40m thick; generally 8-31m. Peritidal to shallow subtidal deposits. Appears as Linnekar Sandstone in Fig.33.3. Ordian age. Hosts a number of uneconomic base metal anomalies.||Negri Subgroup.||Conformably overlies Nelson Shale. Is overlain conformably and gradationally by Panton Formation.|Microbial, bioclast and oncoid limestone, alternating with fossiliferous grey to olive-brown mudstone and marl. Low-diversity fauna of trilobite Redlichia forresti, hyolith Guduguwan hardmani, and brachiopods.|12-JUL-16
10441|Linnekar Limestone|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale|
10441|Linnekar Limestone|69673|5|Briefly described|p142, p192, p193|Cambrian|Cambrian|40m thick.||Negri Subgroup||Overlain by Panton Formation, overlies Nelson Shale|Microbial, bioclast and oncoid limestones alternating with fossiliferous mudstone and marl.|
10441|Linnekar Limestone|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale.|
10441|Linnekar Limestone|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|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.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Basal micritic limestone; middle trilobitic shale; upper limestone and shale|
10441|Linnekar Limestone|71800|5|Briefly described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin.||Negri Subgroup||Overlies the Nelson Shale. Overlain by the Panton Formation.||
10441|Linnekar Limestone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Nelson Shale, underlies the Panton Formation.||
10524|Lloyd Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Pinkerton Sandstone; overlain by Spencer Sandstone. Geological Province: Victoria Basin.||||||25-JAN-06
10524|Lloyd Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
10524|Lloyd Creek Formation|32307|4|Described|Table 2|||Proterozoic||||||
10524|Lloyd Creek Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
10524|Lloyd Creek Formation|32660|5|Briefly described|Table 6|||||||||
10524|Lloyd Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Dolomite, oolitic and stromatolitic; sandy and silty dolomite; siltstone.||||||02-DEC-04
10524|Lloyd Creek Formation|32700|4|Described|Table 1|||Lithology p14. Re: Randal (1962).||||||30-OCT-06
10524|Lloyd Creek Formation|32701|4|Described|Table 1|||Adelaidean. Auvergne Gp. See p9.||||||30-OCT-06
10524|Lloyd Creek Formation|32728|6|Mentioned|Fig.14|||||||||
10524|Lloyd Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10524|Lloyd Creek Formation|45112|6|Mentioned|Table 6|||||||||
10524|Lloyd Creek Formation|48938|2|Defined|p47|Proterozoic|Proterozoic|Measured section p96. ?Adelaidean||||||30-OCT-06
10524|Lloyd Creek Formation|48942|3|Fully described|p71|||||||||
10524|Lloyd Creek Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Pinkerton Sandstone. Overlain by Spencer Sandstone. Oolitic and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone.||||||
10524|Lloyd Creek Formation|60682|4|Described|p9 Table 2, 10|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Pinkerton Sandstone. Conformably overlain by Spencer Sandstone. Max. thickness: 162m. Geological Province: Victoria Basin. Dolostone, dololutite, dolarenite, dolomitic siltstone, quartz sandstone.||||||
10524|Lloyd Creek Formation|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
10524|Lloyd Creek Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Ooidal and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone||||||
10524|Lloyd Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Pinkerton Sandstone. Is overlain by Spencer Sandstone.||
10524|Lloyd Creek Formation|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Ooidal and microbial dolostone, quartzitic and silty dolostone, sandstone, dolomitic siltstone.|
10524|Lloyd Creek Formation|68733|6|Mentioned|p177 Fig.2, p189 Fig.8|Cryogenian|Cryogenian|Victoria Basin.||Of the Auvergne Group.||||05-DEC-17
10524|Lloyd Creek Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Pinkerton Sandstone. Is overlain by Spencer Sandstone.||12-JUL-16
10524|Lloyd Creek Formation|69441|5|Briefly described|p26:2-5|Neoproterozoic|Neoproterozoic|Typically <90m thick, up to 162m locally. Shallow-marine, mixed carbonate/siliciclastic with wave action, storm deposits and brine-logging of sediments.||Auvergne Group.||Conformably overlies Pinkerton Sandstone. Is overlain conformably by Spencer Sandstone.|Dolostone (oolitic and microbial), quartzose and silty dolostone, dololutite, dolarenite, dolomitic siltstone, quartz sandstone. Rare glauconite grains.|12-JUL-16
10524|Lloyd Creek Formation|69673|5|Briefly described|p188|||162m thick.||Auvergne Group|||Oolitic and stromatolitic dolostone interbedded with dolarenite, quartzic dolostone and rippled quartz sandstone.|
10524|Lloyd Creek Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Oolitic and microbial dolostone, quartzic and silty dolostone, sandstone, dolomitic siltstone.|
10524|Lloyd Creek Formation|71302|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|Of Victoria Basin.||Unit of Auvergne Group.||Overlain by Spencer Sandstone. Underlain by Pinkerton Sandstone.||
10524|Lloyd Creek Formation|73083|6|Mentioned|p8|||||||||
10561|Locker Shale|7142|6|Mentioned|p354.|Early Triassic|Early Triassic|Northern Carnarvon Basin, deposited during a marine transgression.||||||
10561|Locker Shale|12466|5|Briefly described|p178.|Middle Triassic|Early Triassic|Marine shales. Poor hydrocarbon source potential and is currently marginal to early mature.||||Is overlain by Mungaroo Formation.||03-SEP-14
10561|Locker Shale|12471|5|Briefly described|p475 Fig.2.|Middle Triassic|Early Triassic|Reached maturity as early as Jurassic and probably expelled hydrocarbons into neighbouring units.|||Cunaloo Member|Overlies Kennedy Group. Is overlain by Mungaroo Formation.||24-OCT-14
10561|Locker Shale|13242|6|Mentioned|p225|Early Triassic|Early Triassic|Contemporaneous with deposition of Lower Mount Goodwin Formation in the Bonaparte Basin. Geological Province: Carnarvon Basin.||||||07-FEB-11
10561|Locker Shale|13255|5|Briefly described|p369|Middle Triassic|Permian|Roebuck Basin. Part of the Westralian 1 petroleum super-system: discussed in detail.||||Is overlain by Keraudren Formation. Is interbedded with Rowley Volcanics.||
10561|Locker Shale|13615|3|Fully described|p3-4, p6-8, p13, 16, 17, 18|Anisian|Induan|Peedamullah Shelf. Up to 596m thick. Spores/Pollen Zone and Dinoflagellate zones provided. Thickness greatly increases towards the depocentre of the Barrow Sub-basin. Deposited in a transgressive shallow marine environment. Intersected in numerous drillholes. Type section occurs in Onslow 1 drillhole between 1587 and 2096m. Contains rich microfauna and microflaura but rare macrofossils.  Age said to be Scythian (Protohaploxypinus samoilovichii Zone) to Anisian (Triplexispoites playfordii Zone). See also p20, p23, p27, p29-p31, p34-p35, p39, p41-p42, p44, p47, p49-p51, p54-p55, p58, p65-p70, p73, p78-p80, p84-p85, p102 App. 3, p119, Plates 2, 3.|c. 251 Ma||Includes the Cunaloo Member.|Overlies the Kennedy Group. Conformably overlies the Abdul Sandstone and the Chinty Formation. Conformably overlain by the Mungaroo Formation.|Dark pyritic shale with local sandstone interbeds and basal limestone.|07-FEB-19
10561|Locker Shale|14227|5|Briefly described|p10|Triassic|Triassic|Geological Province: Carnarvon Basin.||||||07-FEB-11
10561|Locker Shale|22703|4|Described|p117,118,Fig.3|Ladinian|Scythian|||||||
10561|Locker Shale|22814|5|Briefly described|fig2|Triassic|Triassic|||||||
10561|Locker Shale|23520|6|Mentioned|p12, p28|||Geological Province: N. Carnarvon Basin, Exmouth Sub-basin.||||||
10561|Locker Shale|23726|5|Briefly described|p8 Fig 2c|Middle Triassic|Early Triassic|Overlying unit Mungaroo Formation. Underlying unit Chinty Formation. Geological Province: Carnarvon Basin.||||||
10561|Locker Shale|23815|4|Described|p290|Middle Triassic|Early Triassic|Geological Province: Carnarvon Basin. Overlying unit: Mungaroo Formation (conformable) and Birdrong Sandstone (unconformable). Max. thickness: 509 m.||||||14-DEC-04
10561|Locker Shale|24059|5|Briefly described|p131|Triassic|Triassic|Geological Province: Barrow Sub-basin.||||||
10561|Locker Shale|24084|5|Briefly described|p146 Fig.2|Middle Triassic|Early Triassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
10561|Locker Shale|24203|5|Briefly described|p302|Early Triassic|Early Triassic|Same unit as Locker Formation?  Geological Province Carnarvon Basin.||||||21-APR-08
10561|Locker Shale|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
10561|Locker Shale|24331|5|Briefly described|p475 Fig.2|Early Triassic|Early Triassic|Unconformably overlies Chinty Formation. Conformably overlain by Mungaroo Formation. Marine. Geological Province: Barrow Sub-basin.||||||
10561|Locker Shale|24351|5|Briefly described|p37, Plate 4 (in pocket)|Middle Triassic|Middle Triassic|Geological Province: Exmouth Sub-basin/Gascoyne Sub-basin.||||||29-APR-13
10561|Locker Shale|24390|6|Mentioned|p22|||Geological Province: Northern Carnarvon Basin.||||||
10561|Locker Shale|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
10561|Locker Shale|29721|6|Mentioned|Table 102|||||||||
10561|Locker Shale|30565|4|Described|p111|||||||||
10561|Locker Shale|31561|4|Described|p37|||See also P34. Early Triassic. Marginal to marine.||||||
10561|Locker Shale|31604|6|Mentioned|p4|||See also P6 & Table 4. L.-M.Triassic||||||
10561|Locker Shale|32024|6|Mentioned|p12|||Triassic||||||
10561|Locker Shale|32025|6|Mentioned|p977|||L. to M. Triassic. Marine.||||||
10561|Locker Shale|32163|6|Mentioned|p279|||Refers Balme (1969)||||||
10561|Locker Shale|32164|6|Mentioned|p488|||||||||
10561|Locker Shale|32165|5|Briefly described|p195|||Younger than Kockatea Sh. Conodonts, age P200.||||||
10561|Locker Shale|32166|6|Mentioned|p157|||Refers type section||||||
10561|Locker Shale|32648|6|Mentioned|p32|||Triassic||||||
10561|Locker Shale|32710|6|Mentioned|p16|||||||||
10561|Locker Shale|32711|6|Mentioned|Fig.3|||||||||
10561|Locker Shale|32714|6|Mentioned|Fig.7|||Triassic||||||
10561|Locker Shale|32715|6|Mentioned|Fig.16|||||||||
10561|Locker Shale|33386|6|Mentioned|Fig.7|||||||||
10561|Locker Shale|33450|6|Mentioned|Fig.5|||||||||
10561|Locker Shale|33453|6|Mentioned|p70|||Stratigraphy.||||||
10561|Locker Shale|33813|6|Mentioned|p4|||See also Figs 5 & 6||||||
10561|Locker Shale|34008|2|Defined|p70|Triassic|Triassic|||||||
10561|Locker Shale|34009|6|Mentioned|Table III|||||||||
10561|Locker Shale|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
10561|Locker Shale|34363|6|Mentioned|p56|||See also Fig.7. Triassic.||||||
10561|Locker Shale|34846|6|Mentioned|Fig.3|||||||||
10561|Locker Shale|35144|6|Mentioned|Fig.5|||||||||
10561|Locker Shale|35282|6|Mentioned|Fig.2|||||||||
10561|Locker Shale|35983|6|Mentioned|Table 27|||||||||
10561|Locker Shale|36112|5|Briefly described|p27|||||||||
10561|Locker Shale|36257|6|Mentioned|Table 2.1|||||||||
10561|Locker Shale|36890|3|Fully described|p290|||||||||
10561|Locker Shale|36899|6|Mentioned|p1085|||See also P1092.||||||
10561|Locker Shale|37812|6|Mentioned|p656|||||||||
10561|Locker Shale|39261|6|Mentioned|p115|||||||||
10561|Locker Shale|39427|4|Described|Table 1|||||||||
10561|Locker Shale|40617|6|Mentioned|p5|||||||||
10561|Locker Shale|40992|6|Mentioned|Fig.8|||||||||
10561|Locker Shale|41170|6|Mentioned|Fig.3|||||||||
10561|Locker Shale|41271|3|Fully described|p109|||||||||
10561|Locker Shale|41436|6|Mentioned|p43|||||||||
10561|Locker Shale|41438|4|Described|p106|||||||||
10561|Locker Shale|41439|4|Described|p119|||||||||
10561|Locker Shale|41440|4|Described|p136|||||||||
10561|Locker Shale|41441|6|Mentioned|p152|||||||||
10561|Locker Shale|41443|4|Described|p163|||||||||
10561|Locker Shale|41444|6|Mentioned|Fig.4|||||||||
10561|Locker Shale|41446|6|Mentioned|Fig.17|||||||||
10561|Locker Shale|41447|6|Mentioned|Fig.3|||||||||
10561|Locker Shale|41732|6|Mentioned|p534|||||||||
10561|Locker Shale|42075|5|Briefly described|Fig.4 P245|||||||||
10561|Locker Shale|42116|5|Briefly described|Fig.1 P6|||||||||
10561|Locker Shale|42463|6|Mentioned|Fig.2 P169|||||||||
10561|Locker Shale|42615|5|Briefly described|p6|||Triassic||||||
10561|Locker Shale|43173|6|Mentioned|12-54||Triassic|||||||
10561|Locker Shale|43712|5|Briefly described|p10|Ladinian|Scythian|||||||
10561|Locker Shale|43722|5|Briefly described|p9|Ladinian|Scythian|||||||
10561|Locker Shale|43724|5|Briefly described|p28|Ladinian|Scythian|||||||
10561|Locker Shale|43826|6|Mentioned|Fig.2,p163|Late Triassic|Late Permian|||||||01-MAR-10
10561|Locker Shale|44143|4|Described|p.434 Table 4-19, p447, p448 Fig.4-106|Middle Triassic|Middle Triassic|>330m thick; shale with minor sandstone and limestone; marine. Lateral equivalent of Blina Shale. Scythian to Anisian.||||||23-NOV-17
10561|Locker Shale|44159|5|Briefly described|Table p.37||Middle Triassic|||||||
10561|Locker Shale|45142|6|Mentioned|p21|||||||||
10561|Locker Shale|46808|6|Mentioned|Table 2|||||||||
10561|Locker Shale|46849|6|Mentioned|Fig. 6|||||||||
10561|Locker Shale|49942|5|Briefly described|p10|Triassic|Triassic|Equivalent to Kockatea Shale. Geological Province: North Carnarvon Basin.||||||
10561|Locker Shale|50085|5|Briefly described|p23 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||
10561|Locker Shale|60377|6|Mentioned|p62|||Geological Province: Carnarvon Basin.||||||07-FEB-11
10561|Locker Shale|60379|6|Mentioned|p125, p126 fig 3|Middle Triassic|Early Triassic|Dampier sub-basin, Carnarvon Basin. Marine. Areally extensive.||||||
10561|Locker Shale|60384|6|Mentioned|p243 Fig 2b|Early Triassic|Early Triassic|Northern Carnarvon Basin.||||||
10561|Locker Shale|60386|6|Mentioned|p297, 300|Early Triassic||Carnarvon Basin. Distal shelf/basin.||||||
10561|Locker Shale|60725|6|Mentioned|p35 Fig.5, p36 Fig.6. |Triassic|Triassic|||||||
10561|Locker Shale|61023|5|Briefly described|p27 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin. See also p29.||||||11-APR-08
10561|Locker Shale|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Middle Triassic|Age: ~235Ma. Geological Province: Northern Carnarvon Basin and Bedout Sub-basin.||||||01-MAR-10
10561|Locker Shale|63929|6|Mentioned|p131 Fig.2.|Middle Triassic|Early Triassic|Barrow Sub-basin, Peedamullah Shelf, Wombat Plateau, Rowley Terrace and Offshore Canning Basin. Primarily marine. A carbonate member near the top correlates with basal Pollard Formation; represents a major marine highstand event across North West Shelf.|||Includes Cunaloo Member.|Is overlain by Mungaroo and Keraudren Formations.||
10561|Locker Shale|63950|5|Briefly described|p336 Fig. 4|Scythian|Scythian|Overlain by Mungaroo Formation. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
10561|Locker Shale|64977|6|Mentioned|p493 Fig.3.|Early Triassic|Early Triassic|Thevenard Island area.||||Is overlain by Mungaroo Formation.||
10561|Locker Shale|65078|5|Briefly described|p35 Fig. 11|Triassic|Triassic|Geological Province: Barrow Sub-basin.||||||29-APR-13
10561|Locker Shale|66124|5|Briefly described|p169, p170 Fig.2|Anisian|Anisian|Present in North Carnarvon Basin, Canning Basin, Wombat Plateau and Rowley Terrace. Underlies Mungaroo (or Keraudren) Formation.||||||
10561|Locker Shale|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes light brown sandstone; dark grey shale.|
10561|Locker Shale|67200|5|Briefly described|p8 fig 6, p48, p54, app 2 p7|Triassic|Triassic|Thermal conductivity of 1.27 W/mK||||Overlies Chinty Formation, overlain by Mungaroo Formation|Limestone and mottled siltstone/shale.|
10561|Locker Shale|67368|6|Mentioned|p209 Fig.4.|Middle Triassic|Early Triassic|||||||
10561|Locker Shale|67970|5|Briefly described|p3, p13.|Early Triassic|Early Triassic|Exmouth Plateau. Deposition in a broad, low relief, rapidly subsiding fluvio-deltaic coastal plain. Organic rich marine equivalents have greatest potential for mature gas source rock facies.||||Is conformably overlain by, and grades upwards into, Mungaroo Formation.||
10561|Locker Shale|69029|6|Mentioned|p328|Triassic|Triassic|Of Canning Basin.||||||
10561|Locker Shale|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|Triassic|Permian|Carnarvon Basin. Maximum thickness likely greater than 509m. Seals the underlying Kennedy Group. Deposited in a deep marine environment. See also Ch3 p15, Ch3 p17-p18, Ch3 p23-p27, Ch3 p35, Ch3 p37, Ch3 p50, Ch3 p52, Ch3 p54, Ch3 p65-p68, Ch3 p73.||||Overlies the Kennedy Group.||
10561|Locker Shale|69297|5|Briefly described|p337, p339, p352|Anisian|Changhsingian|Roebuck Basin. Shale and minor coal intervals are prospective hydrocarbon source rocks. Sandstones are prospective hydrocarbon reservoirs.||||Overlies the Bedout Volcanics. Overlain by the Lower Keraudren Formation.|Shale and minor coal.|
10561|Locker Shale|69689|6|Mentioned|p16|Triassic|Triassic|Northern Carnarvon Basin.||||Is overlain by Mungaroo Formation.||
10561|Locker Shale|69692|6|Mentioned|p3-4|Triassic|Triassic|Carnarvon Basin.||||Is overlain by Mungaroo Formation.||
10561|Locker Shale|70065|5|Briefly described|Rowley:Fig.2;p1-2.Regional:Fig.4;p3,p5-6|Ladinian|Changhsingian|Rowley Sub-basin, Roebuck Basin. Oil- and gas-prone source rocks, while shoreward facies form reservoirs. Has intraformational seals.||||Overlies Bedout Volcanics. Is overlain by Lower Keraudren Formation or Cossigny Member. Equivalent to Kockatea Shale.|Includes transgressive shales.|
10561|Locker Shale|70066|5|Briefly described|Dampier: Fig.2; p2-3. Exmouth: Fig.2|Anisian|Induan|See also Regional: Fig.6; p4, p7-8. Northern Carnarvon Basin. Fluvio-deltaic sediments are a gas-prone source. Has potential as a seal (untested), and for stratigraphic traps including pinch-outs, unconformity sub-crops and transgressive sandstone packages.||||Overlies Chinty Formation. Is overlain conformably (gradationally) by Mungaroo Formation.|Predominantly marine claystone and siltstone with minor paralic sandstone and shelfal limestone.|
10561|Locker Shale|70906|5|Briefly described|p757|Triassic|Triassic|Gorgon Platform.||||Is overlain by Mungaroo Formation.||
10561|Locker Shale|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Southern Carnarvon Basin.||||Overlain by the Mungaroo Formation.|Shale.|
10561|Locker Shale|71623|5|Briefly described|p345 fig 2, p348 Fig 6||Scythian|Carnarvon Basin. Sonic logs and palynology control shown.|||||Shale|
10561|Locker Shale|72260|5|Briefly described|p1, 3, 4, 5, 7, 10, 13, 14, p19-p21|Anisian||North Carnarvon Basin. 200-1000 m thick. Transgressive to regressive? sequence; unconformable basal boundary (above Permian sediments).||||Underlies the Mungaroo Formation, gradational contact.|Marine claystone, siltstone with minor paralic sandstone and shelfal limestone|
10561|Locker Shale|72505|5|Briefly described|p890|Induan|Induan|Southern Carnarvon Basin. Correlates with the P. Microcorpus and P. Crenulata zones.||||Overlies the Chinty Formation.||
10561|Locker Shale|72910|4|Described|p4 Fig.3, p12-13, p18-19.|Triassic|Triassic|Shown as being located in the Peedamullah Shelf.||||Overlies Chinty Formation (Kennedy Group)|Includes shale, interbedded sandstone and siltstone,  with some limestone indicated in lower parts.|
10561|Locker Shale|73564|6|Mentioned|p1223, 1225|Triassic|Permian|Exmouth Plateau, Gascoyne Margin. Olenekian age.||||Is overlain by Mungaroo Formation.||
10562|Lockeridge Shale Member|37460|6|Mentioned|p141|||||||||
10562|Lockeridge Shale Member|38978|6|Mentioned|p156|||||||||18-JAN-07
10623|Long Hole 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
10623|Long Hole Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
10623|Long Hole Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10623|Long Hole Granite|36885|4|Described|p174|||||||||
10623|Long Hole Granite|43281|5|Briefly described|Map legend||Proterozoic|||||||
10623|Long Hole Granite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex|||Coarse, grey, porphyritic granite, biotite gneiss and augen gneiss; blue-grey quartz characteristic.|
10623|Long Hole Granite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite. Foliated, coarse-grained, porphyritic monzogranite and augen gneiss. Age: 1865-1850Ma. In the western zone of the Hooper Complex and Lamboo Complex (Bow River batholith).||||||07-NOV-08
10623|Long Hole Granite|44366|14|Not recorded|p.8, Table 1||Proterozoic|Definition on Tech.File E/52-5.||||||
10623|Long Hole Granite|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971), part of Lamboo Complex.||||||
10623|Long Hole Granite|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
10623|Long Hole Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
10623|Long Hole Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
10623|Long Hole Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Commonly foliated, grey coarse porphyritic biotite granite, with zones of pink-grey biotite gneiss and augen gneiss|
10623|Long Hole Granite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Foliated, coarse-grained, porphyritic metamonzogranite and augen gneiss.|
10623|Long Hole Granite|72437|6|Mentioned|p76|||||Paperbark Supersuite||||
10656|Loongana Formation|22613|6|Mentioned|p18|||||||||
10656|Loongana Formation|22663|5|Briefly described|S97-1 and 2 p3||Early Cretaceous|||||||01-MAR-10
10656|Loongana Formation|42075|5|Briefly described|Fig.10 P250|||||||||
10656|Loongana Formation|42545|1|Redefined|p13|Hauterivian|Berriasian|||||||
10656|Loongana Formation|43026|5|Briefly described|Table 1,p586|||||||||
10656|Loongana Formation|43052|5|Briefly described|Table 2.1|||||||||
10656|Loongana Formation|44133|5|Briefly described|p134|Hauterivian|Valanginian|Conformably overlain by Madura Formation. Originally named 'Loongana Conglomerate'.||||||
10656|Loongana Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
10656|Loongana Formation|61630|6|Mentioned|p555 Fig. 3|Early Cretaceous|Late Jurassic|Geological Province: Eyre Sub-basin.||||||07-APR-09
10656|Loongana Formation|64580|4|Described|map legend||Early Cretaceous|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.||||||09-DEC-08
10656|Loongana Formation|68715|6|Mentioned|p30 Fig.5|Hauterivian|Berriasian|Bight Basin.||||||
10656|Loongana Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Hauterivian|Berriasian|Eyre Sub-basin.||||Overlain by the Madura Formation.|Sandstone, siltstone and shale.|
10656|Loongana Formation|69632|5|Briefly described|p21 Tb.6, p26, p30, p32|Cretaceous|Cretaceous|Gunbarrel, Eucla Basins. Average shear-wave velocities tabulated. 27-49m thick.||Bight Basin Group.||Is overlain by Madura Formation.|A lenticular, conglomeratic, feldspathic, grey-bluish sandstone. Largely unconsolidated and poorly lithified.|
10656|Loongana Formation|69648|4|Described|p20-21, map legend|Early Cretaceous|Early Cretaceous|Of Bight Basin margin. Occurs in drillholes. Thickness: about 18.3 m. Fluviatile continental deposition.||||Disconformably overlain by Madura Formation.|An essentially sandstone unit; ferruginous gradational, cyclically deposited conglomerates and sandstones through to fine clayey silts; may include mud, and be carbonaceous.|
10656|Loongana Formation|70771|5|Briefly described|p2, p27|Cretaceous|Cretaceous|Eucla Basin.||||Conformably overlain by the Madura Formation.|Siliciclastic sedimentary rocks.|
10656|Loongana Formation|70772|4|Described|p2, p4-9, p11-12, p16-17|Hauterivian|Valanginian|Madura Shelf. Nonconformably overlies crystalline basement. Intersected in nine wells and achieves a thickness between 20 and 43m. Petrography is discussed further. Deposited in a high-energy fluvial/lacustrine type environment. Poor sorting and textural immaturity suggest deposition was rapid. Palynology suggests a freshwater/brackish type setting. See also p22-24, p28, p31, p33-34, p36, p41.||||Conformably overlain by the Madura Formation. Disconformably overlies the Decoration Sandstone.|Very poorly consolidated, quartz dominated, feldspathic sand with minor mica. Medium-coarse grained, angular, poorly sorted sand.|
10656|Loongana Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
10656|Loongana Formation|71618|4|Described|p124-125,127-135|Hauterivian|Valanginian|Geological province: Bight Basin, Madura Shelf. Deposited during period of thermal subsidence during the Early Cretaceous. Intersected in 9 wells in the study area. Thickness: 20-40m. Sample in the FOR010 borehole (235.9-235.92 m and 244.3-244.5 m) contained a distinctive and rich Early Cretaceous palynomorph assemblage (see p127 for palynology). U-Pb ICPMS zircon analysis yield major concordant age peaks at c. 1150 and 1650 Ma, similar to the Decoration Sandstone and Madura Formation.||||Conformably overlain by Madura Formation. Underlain by crystalline basement, or Decoration Sandstone where present.|Very poorly consolidated quartz dominated, feldspathic sand with minor mica.|06-SEP-19
10656|Loongana Formation|71891|5|Briefly described|p6-p7, p14, p29, p32-p33, |Early Cretaceous|Middle Jurassic|Bight Basin, Coompana Province. 30-324m thick. Interpreted to represent the initial rift phase of the basin. Deposited in a terrestrial low sinuosity fluvial environment. See also p35-p37, p44-p52, p54-p55.||||Conformably overlain by the Madura Formation.|Semi-solid sand, pebly conglomerate.|
10656|Loongana Formation|72344|5|Briefly described|p4, p9, p13, p49, p61|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324m. Interpreted to represent an initial rift phase in a terrestrial low sinuosity fluvial environment. Intersected in drillhole CDP008. Petrography, SHRIMP analyses and geochemistry are discussed for several samples.Maximum depositional age is derived from SHRIMP dating in this volume. See also p84, p107, p110-p112, p125, p169.|350 +/- 5 (max dep age)|||Conformably overlain by the Madura Formation.|Sandy to shaly succession of cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72465|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens. Up to 324m thick.||||Is overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72466|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Up to 324m thick. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens.||||Is overlain conformably by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72467|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1991, 1995). Bight Basin, Coompana Province. Up to 324m thick. Represents an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens.||||Overlies ?Moodini Supersuite. Is overlain conformably by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72468|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72469|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72470|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72471|5|Briefly described|p8|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72472|5|Briefly described|p8, p17-18, p20-21|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 324 m. Interpreted to represent an initial rift phase in a terrestrial low-sinuosity fluvial environment within isolated grabens of the developing rift valley. Interfingering transition with overlying Madura Formation.||||Conformably overlain by Madura Formation.|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.|
10656|Loongana Formation|72947|6|Mentioned|p16|Early Cretaceous|Early Cretaceous|||||Nonconformably underlain by Koonalda Suite.||
10656|Loongana Formation|73084|5|Briefly described|p16-17|Early Cretaceous|Early Cretaceous|Bight Basin. 10-50 m thick.||||Overlain by Madura Formation.|Poorly consolidated dark carbonaceous shale, siltstone and minor sandstone.|
10656|Loongana Formation|73641|5|Briefly described|p4, 8-15, 17|Early Cretaceous|Early Cretaceous|Bight Basin. ~30m thick. Terrestrial low-sinuosity fluvial environment within isolated grabens in a rift valley. Mineralogical, element, TOC compositions tabulated.||||Underlies and interfingers with Madura Formation.|Sandstones, carbonaceous sandstones, glauconitic sandstones, siltstones, and argillites, commonly pyritic.|
10676|Louisa Downs Group|22496|6|Mentioned|p11||Neoproterozoic|||||||
10676|Louisa Downs Group|22547|6|Mentioned|p28|||Correlates with Albert Edward Group||||||
10676|Louisa Downs Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
10676|Louisa Downs Group|22754|5|Briefly described|p5 Tb. 1|Neoproterozoic|Neoproterozoic|Age c. 610 Ma.  Geological Province: Louisa Basin.||||||
10676|Louisa Downs Group|22764|5|Briefly described|Table1,p6||Adelaidean|||||||01-FEB-10
10676|Louisa Downs Group|23383|4|Described|p20-21, p5 Tb.1|Neoproterozoic|Neoproterozoic|Unconformably overlies rocks of the Lamboo Complex and Kuniandi Group; also unconformably overlies Crowhurst Group Colombo Sst. and Glidden Gp. (on MOUNT RAMSAY).  Age: c.610Ma.  Max thickness: 4000 m.  Geol. Prov: Yampi Orogen. See also p6 Fig. 3.||||||14-APR-08
10676|Louisa Downs Group|23516|6|Mentioned|p599 Fig.6|||||||||
10676|Louisa Downs Group|23599|4|Described|p17|Neoproterozoic|Neoproterozoic|Age: c.610 Ma. Underlain by Lamboo Complex. Geological Province: Louisa Basin. Max. thickness: 4000 m.||||||20-DEC-07
10676|Louisa Downs Group|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes: Lubbock and Tean Formations, McAlly Shale, Yurabi and Egan Formations.  Age: c.670Ma.||||||
10676|Louisa Downs Group|23621|6|Mentioned|p32|||||||||
10676|Louisa Downs Group|23806|5|Briefly described|p1122|||Underlain by Kuniandi Group.||||||
10676|Louisa Downs Group|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Basin. In the MOUNT RAMSAY 1:250,000 sheet area. Correlates with Albert Edward Group||||||06-APR-05
10676|Louisa Downs Group|30097|6|Mentioned|Fig.54|||Also Tables 23,24,25||||||
10676|Louisa Downs Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
10676|Louisa Downs Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10676|Louisa Downs Group|31393|6|Mentioned|Pl.25|||||||||
10676|Louisa Downs Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10676|Louisa Downs Group|32660|4|Described|Table 6|||||||||
10676|Louisa Downs Group|32728|6|Mentioned|Fig.3|||||||||
10676|Louisa Downs Group|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10676|Louisa Downs Group|36551|6|Mentioned|Table 10|||||||||
10676|Louisa Downs Group|36888|4|Described|p214|||||||||
10676|Louisa Downs Group|36898|6|Mentioned|p188|||||||||
10676|Louisa Downs Group|37299|6|Mentioned|Fig.1|||||||||
10676|Louisa Downs Group|37462|4|Described|Table 4.X|||||||||
10676|Louisa Downs Group|37927|6|Mentioned|p504|||||||||
10676|Louisa Downs Group|38157|6|Mentioned|Table X|||||||||
10676|Louisa Downs Group|38243|6|Mentioned|p357|||||||||
10676|Louisa Downs Group|38988|6|Mentioned|Fig.4|||||||||
10676|Louisa Downs Group|39210|5|Briefly described|p49|||||||||
10676|Louisa Downs Group|40105|6|Mentioned|p313|||||||||
10676|Louisa Downs Group|42811|6|Mentioned|p30|||||||||
10676|Louisa Downs Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
10676|Louisa Downs Group|43595|6|Mentioned|Fig.5-34,p551|||||||||
10676|Louisa Downs Group|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
10676|Louisa Downs Group|44140|4|Described|p299-300, p301 fig 4-7, p303 Tb. 4-2|Neoproterozoic|Neoproterozoic|Dow and Gemuts (1969). Of Mount Ramsay area. Glacial; correlated with glacial successions in the Mount House and Osmond Range areas. Associated with the 676 Ma Marinoan glaciation.|||Egan, Yurabi, Tean, Lubbock Formations; McAlly Shale.|Overlies Kuniandi Group unconformably.|Basal diamictite overlain by a thin persistent dolomite unit that passes up into thick sequences of mostly green or grey siltstone, shale and sandstone.|07-MAR-18
10676|Louisa Downs Group|44155|6|Mentioned|p250, p254 Fig.3-40|Neoproterozoic|Neoproterozoic|Glacial sequence.||||||
10676|Louisa Downs Group|44231|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Egan and Yurabi Formations, McAlly Shale and the Tean and Lubbock Formations. Geological Province: Louisa Basin.||||||19-MAY-05
10676|Louisa Downs Group|44397|14|Not recorded|p.15,20||Adelaidean|Defn. on Tech.File E/52-9. See also p.6,10,Fig.4, Table 3.||||||
10676|Louisa Downs Group|44398|14|Not recorded|map legend||Adelaidean|||||||
10676|Louisa Downs Group|44693|5|Briefly described|Map Legend||Proterozoic|||||||
10676|Louisa Downs Group|44694|5|Briefly described|Map Legend||Proterozoic|||||||
10676|Louisa Downs Group|45047|2|Defined|p36|Adelaidean|Adelaidean|||||||
10676|Louisa Downs Group|45140|6|Mentioned|p13|||Kimberley region.|~660 Ma.|||||
10676|Louisa Downs Group|48927|2|Defined|p16|Adelaidean|Adelaidean|||||||
10676|Louisa Downs Group|60724|6|Mentioned|p5 Fig. 2|Neoproterozoic|Neoproterozoic|||||||
10676|Louisa Downs Group|61574|5|Briefly described|p690|Neoproterozoic III|Neoproterozoic III|Unconformably overlies the Crowhurst Group.||||||07-JAN-10
10676|Louisa Downs Group|63458|6|Mentioned|p872 Fig.1, p873 Fig.2, p874. |Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region. ~4000 m thick. See also p880 Fig.6, p882 Fig.8, p897 Fig.19.|||Includes Egan, Yurabi, Tean and Lubbock Formations; McAlly Shale.||Package of quartz sandstone, silty sandstone and siltstone; very minor dolomite and rare diamictite at base.|
10676|Louisa Downs Group|63762|5|Briefly described|p19|||Silicilcastic package overlain by Antrim Plateau Volcanics. Includes Egan Formation.||||||07-FEB-11
10676|Louisa Downs Group|64104|6|Mentioned|p70 fig 7|Neoproterozoic|Neoproterozoic|||||||
10676|Louisa Downs Group|64580|4|Described|map legend|Ediacaran|Ediacaran|Undivided, siltstone, sandstone, quartz wacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite.||||||09-DEC-08
10676|Louisa Downs Group|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley.|||Includes Lubbock, Tean, Yurabi, Egan Formations; McAlly Shale.|Overlain by the Antrim Plateau Volcanics. Underlain by the Kuniandi Group.||27-MAY-15
10676|Louisa Downs Group|67620|5|Briefly described|p2-3, 5|Ediacaran|Ediacaran|Crops out in the Mount Ramsay area, Kimberley region.|||Egan, Yurabi, Tean, Lubbock Formations; McAlly Shale.|Overlies Kuniandi Group. Is overlain by Antrim Plateau Volcanics.||
10676|Louisa Downs Group|68138|6|Mentioned|p154, 156|Neoproterozoic|Neoproterozoic||||Egan, Yurabi, Tean, Lubbock Formations; McAlly Shale.|||
10676|Louisa Downs Group|68244|4|Described|p659-660,662-666|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. Crops out extensively on the margins of the O'Donnell and Louisa Synclines.|||Includes Lubbock Formation, Tean Formation, McAlly Shale, Yurabi Formation and Egan Formatrion.|Overlain unconformably by Antrim Plateau Volcanics. Underlain disconformably by Kuniandi Group.|Dolomite, diamictite, conglomerate and sandstone at the base, overlain by a thick package of rippled sandstone and black, green and purple mudstone and siltstone with interbeds of conglomerate and greywacke.|
10676|Louisa Downs Group|68473|6|Mentioned|p530-531|Neoproterozoic|Neoproterozoic|Mount Ramsay.|||Includes Egan Formation, Yurabi Formation, McAlly Shale, Tean Formation, Lubbock Formation, Antrim Plateau Volcanics.|||
10676|Louisa Downs Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut.csv|Ediacaran|Ediacaran||||||Undivided: siltstone, sandstone, quartz wacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone and tillite.|
10676|Louisa Downs Group|68733|6|Mentioned|p189 Fig.8|||||||||
10676|Louisa Downs Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
10676|Louisa Downs Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin|||Includes Lubbock Formation, Tean Formation, McAlly Shale, Yurabi Formation, Egan Formation.||Siltstone, sandstone, quartzwacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite.|31-JUL-15
10676|Louisa Downs Group|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 500k_geologyp08_lut.csv.|||Includes Lubbock Formation, Tean Formation, McAlly Shale, Yurabi Formation, Egan Formation||Undivided; siltstone, sandstone, quartz wacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone and tillite.|
10676|Louisa Downs Group|69587|5|Briefly described|500k_geologyp08_lut.csv|Ediacaran|Ediacaran||||||Undivided, siltstone, sandstone, quartz wacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite|
10676|Louisa Downs Group|69597|6|Mentioned|p5 fig 2b|||||||||
10676|Louisa Downs Group|69634|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Of Louisa 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.|850-635 Ma (Inferred)||Includes Egan Formation, McAlly Shale, Tean Formation, Yurabi Formation.||Undivided, siltstone, sandstone, quartz wacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite|
10676|Louisa Downs Group|70154|6|Mentioned|100k_interpgeop_lut.csv||||||Includes Lubbock Formation, Tean Formation, McAlly Shale, Yurabi Formation, Egan Formation|||
10676|Louisa Downs Group|70731|5|Briefly described|p268|Neoproterozoic|Neoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||Equvalent to Mount House Group.||
10676|Louisa Downs Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 3 and 4, Centralian Superbasin.||||||20-APR-20
10676|Louisa Downs Group|70851|6|Mentioned|p19|||||||||
10676|Louisa Downs Group|71146|5|Briefly described|p6, p21|Cambrian|Cambrian|Bonaparte Basin. Up to 3.7 km thick. Age is tentative.||||Overlies the Egan Formation. Unconformably overlain by the Antrim Plateau Volcanics.|Mixed sandstone, mudstone and coal.|
10676|Louisa Downs Group|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, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|635-541 Ma (inferred)||Includes Lubbock Formation, Egan Formation, McAlly Shale, Tean Formation, Yurabi Formation, Bunganura Beds.||Siltstone, sandstone, quartzwacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite|
10676|Louisa Downs Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Louisa Basin.  Age from biostratigraphy.|||||Siltstone, sandstone, quartzwacke, pebble conglomerate, shale, dolomite, stromatolitic dolomite, limestone, and tillite.|
10834|Lubbock Formation|23383|4|Described|p21, p18 Tb. 2|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group.  Medium-grained quartz wacke, siltstone. Conformably overlies Tean Formation. Max. thickness: >1830 m.  Geological Province: Louisa Basin.||||||30-NOV-06
10834|Lubbock Formation|23599|4|Described|p17|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group.  Underlying unit Tean Formation. Geological Province: Louisa Basin. Max. thickness: 1830 m.||||||
10834|Lubbock Formation|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Grey, green or purple siltstone and shale; interbedded with fine- and medium-grained quartz wacke.||||||25-JAN-05
10834|Lubbock Formation|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group.||||||
10834|Lubbock Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10834|Lubbock Formation|32728|6|Mentioned|Table 7|||See also Fig.16||||||
10834|Lubbock Formation|36551|6|Mentioned|Table 10|||||||||
10834|Lubbock Formation|36888|4|Described|p214|||||||||
10834|Lubbock Formation|36898|5|Briefly described|Table IV|||See also Fig.2B||||||
10834|Lubbock Formation|37927|6|Mentioned|p510|||||||||
10834|Lubbock Formation|38157|6|Mentioned|Table X|||||||||
10834|Lubbock Formation|41429|6|Mentioned|p247|||||||||
10834|Lubbock Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Cryogenian|Cryogenian|Of Mount Ramsay area. 1830m thick.||Louisa Downs Group||Conformably overlies Tean Formation. Probably equivalent to Flat Rock Formation.|Grey, green or purple siltstone and shale and interbedded sub-greywacke; some dolomite.|07-MAR-18
10834|Lubbock Formation|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group. Grey, green or purple siltstone and shale; interbedded with fine- and medium-grained quartz wacke. Age: <610Ma. Geological Province: Louisa Basin.||||||19-MAY-05
10834|Lubbock Formation|44397|14|Not recorded|p.15,20, Table 3||Adelaidean|Louisa Downs Group. Defn. on Tech.File E/52-9.||||||
10834|Lubbock Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
10834|Lubbock Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
10834|Lubbock Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
10834|Lubbock Formation|45047|4|Described|p36|||||||||
10834|Lubbock Formation|48927|2|Defined|p31|Adelaidean|Adelaidean|||||||
10834|Lubbock Formation|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Louisa Downs Group.||||
10834|Lubbock Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley.||Of the Louisa Downs Group.||Overlain by Antrim Plateau Volcanics. Underlain by Tean Formation.||
10834|Lubbock Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||Overlies Tean Formation. Is overlain by Antrim Plateau Volcanics.||
10834|Lubbock Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||||
10834|Lubbock Formation|68244|4|Described|p660,665|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. Up to 2000m thick.||Unit of Louisa Downs Group.||Uppermost unit of Louisa Downs Group. Underlain by Tean Formation.|Medium-grained quartz wackestone and siltstone|
10834|Lubbock Formation|68473|6|Mentioned|p531|||Mount Ramsay. Part of the postglacial succession.||Louisa Downs Group||||
10834|Lubbock Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin||Louisa Downs Group|||Grey, green or purple siltstone and shale; interbedded with fine- and medium-grained quartz wacke.|31-JUL-15
10834|Lubbock Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Grey, green or purple siltstone and shale; interbedded with fine and medium grained quartz wacke.|
10834|Lubbock Formation|69634|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Of Louisa Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|850-635 Ma (Biostrat)|Unit of Louisa Downs Group.|||Grey, green or purple siltstone and shale; interbedded with fine- and medium-grained quartz wacke|
10834|Lubbock Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Louisa Downs Group|||Siltstone and shale; interbedded with fine and medium grained quartz wacke.|
10834|Lubbock 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.|||Grey, green or purple siltstone and shale; interbedded with fine- and medium-grained quartz wacke|
10840|Lucas Formation|22446|6|Mentioned|p20|Mesozoic|Mesozoic|||||||
10840|Lucas Formation|29809|6|Mentioned|Table 1|||||||||
10840|Lucas Formation|29810|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|29812|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|29817|5|Briefly described|p7|||||||||
10840|Lucas Formation|29819|6|Mentioned|Map legend|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
10840|Lucas Formation|31360|4|Described|Table 1|||||||||
10840|Lucas Formation|31362|4|Described|Table 1|||||||||
10840|Lucas Formation|35205|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|36473|6|Mentioned|Map legend|Permian|Permian|||||||
10840|Lucas Formation|36532|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
10840|Lucas Formation|41883|6|Mentioned|p65|||||||||
10840|Lucas Formation|42504|5|Briefly described|Table 4 P73|||||||||
10840|Lucas Formation|43631|6|Mentioned|p27|||||||||
10840|Lucas Formation|45140|2|Defined|p13-14, p26, p40, p46, p49, p61-64, p68|Paleozoic|Paleozoic|See also p75, p83, Appx.p42-43. Hodgson (1976). Previously the Lucas Beds (Casey and Wells, 1964). Named after Lake Lucas. Flat or gently-dipping. Type section (described in some detail) is a low cliff at 20deg 53'30"S, 28deg 56'00"E in the Lucas sheet area. Casey and Wells (1964) chose the bed of Lake Dennis as the "nominate" exposure, but no rocks of the Formation are exposed as they are covered by salt and alluvium. Estimated 1000m thick. Unfossiliferous: probably lacustrine. Local calcrete and laterite cappings. Source of salty water from bores. Correlated with Pertnjara Group; suggested correlation with Noonkanbah Formation is dubious. Possibly Devonian.||||Inferred to overlie Muriel Range Sandstone and Erica Sandstone unconformably. Is overlain unconformably by Pedestal Beds.|Purplish to grey, medium- to fine-grained friable calcareous sandstone; medium- to coarse-grained non-calcareous sandstone (lithic to sublithic arenite); thin-bedded to laminated siltstone and mudstone; local thin limestone beds and sandy dolomite.|
10840|Lucas Formation|45155|6|Mentioned|p42|||||||||
10840|Lucas Formation|46864|4|Described|p38|||||||||
10840|Lucas Formation|50315|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone.  Age: <410Ma.||||||09-JUN-04
10840|Lucas Formation|50374|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone.||||||
10840|Lucas Formation|50376|5|Briefly described|Map Legend|Devonian|Devonian|Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.||||||19-APR-06
10840|Lucas Formation|60676|5|Briefly described|Map legend|Devonian|Devonian|Calcareous and non calcareous sandstone, siltstone and mudstone; minor limestone.||||||19-JAN-05
10840|Lucas Formation|61861|5|Briefly described|p4, Map 1|Devonian|Devonian|Flat-lying siliciclastic rocks.||||Overlies Antrim Plateau Volcanics.||03-APR-12
10840|Lucas Formation|62377|5|Briefly described|p15|||Overlies the Dead Bullock Formation.||||||
10840|Lucas Formation|62628|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Geological Province: Canning Basin. Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.||||||07-NOV-08
10840|Lucas Formation|64580|4|Described|map legend||Paleozoic|Sandstone, in part calcareous, siltstone, mudstone; minor limestone and conglomerate.||||||09-DEC-08
10840|Lucas Formation|64675|6|Mentioned|p10, Map 1|||||||||19-MAR-14
10840|Lucas Formation|65074|4|Described|p350 fig 4-36, p351, p358-360, p362|Paleozoic|Paleozoic|See also p353, p359 fig 4-13, p360, p362. Of Birrindudu Basin. 1000 m thick. Non-fossiliferous; possibly Devonian. Type section is a cliff exposure along E shore of Lake Dennis, 20o54'S, 128o56'E.||||Overlain by Pedestal beds (unconformably). Overlies Redcliff Pound Group (unconformably). Probably correlates with Pertnjara Group.|Sandstone (calcareous or not), siltstone, mudstone; minor dolomite, limestone.|
10840|Lucas Formation|65324|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65349|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65350|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|65351|6|Mentioned|Map legend|Devonian|Devonian|Not shown on map||||||
10840|Lucas Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleozoic|Paleozoic|Canning Basin. See also 500k_geologyp08_lut.csv.|||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate.|
10840|Lucas Formation|69432|6|Mentioned|p17:2|||Canning Basin.||||Overlies Birrindudu Group.||12-JUL-16
10840|Lucas Formation|69440|5|Briefly described|p25:2|Devonian|Devonian|Canning Basin.||||Unconformably overlies Erica Sandstone.||12-JUL-16
10840|Lucas Formation|69453|5|Briefly described|p37:1|Devonian|Devonian|Lucas Outlier, Canning Basin. Deposition in a fluvio-lacustrine environment. Estimated thickness of 1000m. Age inferred from correlation with Pertnjara Group (Amadeus Basin).||||Unconformably overlies (inferred) Redcliff Pound Group. Is inferred to be overlain unconformably by Pedestal beds. (Inferred) correlative of Pertnjara Group.|Flat-lying to gently-dipping, medium- to fine-grained calcareous to non-calcareous sandstone, interbedded with siltstone and mudstone, which are locally calcareous. No marine fossils.|12-JUL-16
10840|Lucas Formation|69587|4|Described|GEOL_LUT_CSV files|Paleozoic|Paleozoic|Of Canning Basin. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|541-252.17 Ma (inferred)||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate|
10840|Lucas Formation|69673|5|Briefly described|p200|||Approximately 1000m thick.|||||Medium to fine grained calcareous to non-calcareous sandstone interbedded with siltstone and mudstone, which are locally calcareous.|
10840|Lucas Formation|70130|5|Briefly described|Map legend|Paleozoic|Paleozoic|Canning Basin.|||||Sandstone (partly calcareous), siltstone and mudstone; minor limestone and conglomerate.|
10840|Lucas Formation|70826|6|Mentioned|p6 tbl 3, p11|Paleozoic|Paleozoic|eastern Canning Basin.||||||20-MAY-20
10840|Lucas Formation|70852|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Canning Basin.|||||Calcareous and non-calcareous sandstone, siltstone and mudstone; minor limestone.|
10840|Lucas Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
10840|Lucas Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleozoic|Paleozoic|Canning Basin. Age inferred.|||||Sandstone (partly calcareous), siltstone, and mudstone; minor limestone and conglomerate|
10840|Lucas Formation|73445|5|Briefly described|p3, 6, 8, 10, 24, 35, 37-38, 41-43|Paleozoic|Paleozoic|See also p65-118. Canning Basin. Regolith chemistry tabulated. Bedrock appears to control regolith chemistry in this unit.|||||Thin-bedded calcareous sandstone, siltstone, mudstone, minor limestone and conglomerate.|
10861|Lulworth beds|40356|6|Mentioned|p7|||Informal nomenclature||||||
10863|Luman Siltstone|22547|6|Mentioned|p21|||||||||
10863|Luman Siltstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
10863|Luman Siltstone|23751|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 75 m.||||||07-NOV-08
10863|Luman Siltstone|30097|6|Mentioned|Table 23|||||||||
10863|Luman Siltstone|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10863|Luman Siltstone|30533|5|Briefly described|p15|||On Table 2||||||
10863|Luman Siltstone|30894|5|Briefly described|p250|||Carpentarian||||||
10863|Luman Siltstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10863|Luman Siltstone|30896|4|Described|p16|||||||||
10863|Luman Siltstone|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
10863|Luman Siltstone|31404|6|Mentioned|Fig.1|||||||||
10863|Luman Siltstone|32660|5|Briefly described|Table 3|||||||||
10863|Luman Siltstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
10863|Luman Siltstone|32728|5|Briefly described|p34|||See also Table 5||||||
10863|Luman Siltstone|34462|6|Mentioned|p8|||||||||
10863|Luman Siltstone|36551|6|Mentioned|Table 10|||||||||
10863|Luman Siltstone|37462|6|Mentioned|Fig.4.9|||||||||
10863|Luman Siltstone|41158|6|Mentioned|p65|||||||||
10863|Luman Siltstone|41557|6|Mentioned|p589|||||||||
10863|Luman Siltstone|41987|5|Briefly described|Fig.4 P74|||||||||
10863|Luman Siltstone|42149|6|Mentioned|Table 1 P709|||||||||
10863|Luman Siltstone|42710|5|Briefly described|map legend|Proterozoic||||||||
10863|Luman Siltstone|42811|5|Briefly described|p21|||of Speewah Group||||||
10863|Luman Siltstone|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
10863|Luman Siltstone|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
10863|Luman Siltstone|44140|5|Briefly described|p295, p297 fig 4-4|Paleoproterozoic|Paleoproterozoic|Up to 95 m thick.||Speewah Group||Overlies O'Donnell Formation.|Micaceous siltstone, shale; minor sandstone; mud cracks, ripple marks, cross beds.|07-MAR-18
10863|Luman Siltstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
10863|Luman Siltstone|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group. Purple-grey shale, grey micaceous siltstone, silty shale, and fine-grained sandstone. Age: c.1835Ma. Geological Province: Speewah Basin.||||||07-NOV-08
10863|Luman Siltstone|44317|4|Described|Table 2||Carpentarian|||||||
10863|Luman Siltstone|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
10863|Luman Siltstone|44363|5|Briefly described|p.6,11,12,13|||(Carpentarian) Speewah Group.||||||
10863|Luman Siltstone|44364|14|Not recorded|map legend|||||||||
10863|Luman Siltstone|44366|14|Not recorded|p.14, Table 2||Carpentarian|Part of Speewah Group.||||||
10863|Luman Siltstone|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Speewah Group.||||||
10863|Luman Siltstone|44397|14|Not recorded|p.17, Table 2||Carpentarian|Speewah Group.||||||
10863|Luman Siltstone|44398|14|Not recorded|map legend||Carpentarian|||||||
10863|Luman Siltstone|44868|5|Briefly described|Map Legend||Proterozoic|||||||
10863|Luman Siltstone|45047|5|Briefly described|p28|||||||||
10863|Luman Siltstone|48931|3|Fully described|p49|||||||||
10863|Luman Siltstone|60714|5|Briefly described|p111, p113 Fig.2. |||Originally the topmost unit in Speewah Group, conformably overlain by King Leopold Sandstone at base of Kimberley Group.  Conglomerate over a low-angle unconformity within this latter unit (Williams 1969) resulted in recognition of Bedford Sandstone as top of Speewah Group.||Unit in Speewah Group.||Overlies Lansdowne Arkose. Is intruded by Hart Dolerite. Is overlain by Bedford Sandstone.||21-JUL-15
10863|Luman Siltstone|64748|5|Briefly described|p269 Fig 2|||Of the Speewah Group; Underlies the Bedford Sandstone; overlies the Lansdowne Arkose||||||
10863|Luman Siltstone|67563|6|Mentioned|p122 Fig.2|||||Of the Speewah Group.||||21-JUL-15
10863|Luman Siltstone|68078|5|Briefly described|p6 figure 3, p8, p23|Paleoproterozoic|Paleoproterozoic|||Speewah Group||Overlies Tunganary Formation, overlain by Lansdowne Arkose|Siltstone.|13-SEP-22
10863|Luman Siltstone|68992|6|Mentioned|p498 Fig.1|||Speewah Basin.||Of the Speewah Group.||||
10863|Luman Siltstone|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|||Speewah Group.||Overlies Lansdowne Arkose. Is overlain by Bedford Sandstone.||
10863|Luman Siltstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin.Unit relationships from geochron file 182106.1.pdf.||Speewah Group||Conformably overlies Lansdowne Arkose.|Green and brown siltstone, mudstone, and thin-bedded sandstone; ferruginous, micaceous siltstone|21-JUL-15
10863|Luman Siltstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Speewah Group|||Green and brown siltstone, mudstone and thin bedded sandstone; ferruginous micaceous siltstone.|
10863|Luman Siltstone|69585|5|Briefly described|p4-5|Orosirian|Orosirian|||Speewah Group.||Conformably overlies Lansdowne Arkose.||13-JUN-17
10863|Luman Siltstone|69634|4|Described|GEOL_LUT_CSV files|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 100k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1835-1784 Ma (Inferred)|Unit of Speewah Group.||Underlain conformably by Landsdowne Arkose.|Green and brown siltstone, mudstone, and thin-bedded sandstone; ferruginous, micaceous siltstone|
10863|Luman Siltstone|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.||Unit in Speewah Group.|||Green and brown siltstone, mudstone and thin-bedded sandstone; ferruginous, micaceous siltstone.|
10863|Luman Siltstone|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.||Speewah Group.||Overlies Lansdowne Arkose.|Green and brown siltstone, mudstone, and thin-bedded sandstone; ferruginous, micaceous siltstone.|
10863|Luman Siltstone|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv.|1797- 1835 Ma|Speewah Group|||Green and brown siltstone, mudstone, and thin-bedded sandstone; ferruginous, micaceous siltstone.|
10863|Luman Siltstone|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, 1m_geologyl12_lithology_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyl12_lut.csv.|1835-1797 Ma (inferred)|Unit of Speewah Group.||Underlain conformably by Lansdowne Arkose.|Recessive rippled red-brown to grey-green micaceous siltstone and phyllite interbedded with fine feldspathic sandstone|
10863|Luman Siltstone|71281|4|Described|p421|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Speewah Basin. Up to 75m thick.||Speewah Group.||Overlies Lansdowne Arkose. Is overlain by Bedford Sandstone.|Rippled red-brown to grey-green micaceous siltstone and phyllite interbedded with fine feldspathic sandstone.|
10863|Luman Siltstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.|||Green and brown siltstone, mudstone, and thin-bedded sandstone; ferruginous, micaceous siltstone.|
10863|Luman Siltstone|72490|5|Briefly described|p3-4|||Maximum thickness of 75 m.||Speewah Group|||Rippled red-brown to grey-green micaceous siltstone and phyllite interbedded with fine feldspathic sandstone.|
10869|Lunnon Basalt|22534|6|Mentioned|Fig.5 p10|||Of Kalgoorlie Group.||||||21-OCT-08
10869|Lunnon Basalt|22666|3|Fully described|p695, Fig.1b p696|Archean|Archean|Age of unit 2710 Ma. See also p697-704, Fig.2 p697||||||07-NOV-08
10869|Lunnon Basalt|22672|6|Mentioned|P276|||||||||
10869|Lunnon Basalt|23130|5|Briefly described|p348|||||||||
10869|Lunnon Basalt|23137|4|Described|p245 Table.2|||Of Kalgoorlie Group.||||||14-APR-08
10869|Lunnon Basalt|23786|5|Briefly described|p10|Archean|Archean|Of Kambalda Group. Geological Province: Yilgarn Craton.||||||07-NOV-08
10869|Lunnon Basalt|23926|5|Briefly described|p17|||||||||
10869|Lunnon Basalt|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
10869|Lunnon Basalt|24196|5|Briefly described|p47 Fig.5|||Overlain by the Kambalda Komatiite. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||28-MAY-04
10869|Lunnon Basalt|24322|5|Briefly described|p58, p72 Fig. 11|Archean|Archean|Underlies: Kambalda Komatiite Formation.  Of the Kambalda Group.||||||07-NOV-08
10869|Lunnon Basalt|24325|5|Briefly described|p58|||Of the Kambalda Group. Overlain by the Kambalda Komatiite Formation. Geological Province: Kambalda Dome, Yilgarn Craton.||||||
10869|Lunnon Basalt|41368|6|Mentioned|p73|||See also P73||||||
10869|Lunnon Basalt|41644|6|Mentioned|p219|||||||||
10869|Lunnon Basalt|41670|6|Mentioned|p249|||||||||
10869|Lunnon Basalt|41890|5|Briefly described|p278|||||||||
10869|Lunnon Basalt|42117|6|Mentioned|p65|||See also Table 1||||||
10869|Lunnon Basalt|42221|6|Mentioned|p25|||||||||
10869|Lunnon Basalt|42406|5|Briefly described|Fig.2 P250|||||||||
10869|Lunnon Basalt|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
10869|Lunnon Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
10869|Lunnon Basalt|42870|5|Briefly described|Table 1, P67|||||||||
10869|Lunnon Basalt|43102|5|Briefly described|p11|||||||||
10869|Lunnon Basalt|43162|6|Mentioned|5|||||||||
10869|Lunnon Basalt|43496|6|Mentioned|6-15|||Age: 2702+/-4Ma.||||||21-OCT-08
10869|Lunnon Basalt|60514|4|Described|p26 Fig. 3, p28, p36 Fig. 6, p65 Tb. 1|Archean|Archean|Of the Kalgoorlie Group. Conformably overlain by the Silver Lake Member of the Kambalada Komatiite. Age: 2726+/-30 Ma. Maximum thickness: 5000m. Tholeiitic basalt sequence Geological Province: Kambalda Domain, Yilgarn Craton.||||||07-FEB-11
10869|Lunnon Basalt|60555|6|Mentioned|p5, p6 Fig. 3|Archean|Archean|Overlain by Kambalda Komatiite. Thickness: 1900m.||||||07-NOV-08
10869|Lunnon Basalt|60578|5|Briefly described|p5|Archean|Archean|Age: c. 2.7Ga||||||07-NOV-08
10869|Lunnon Basalt|60623|4|Described|p25 Fig.2, p28|Archean|Archean|Age: 2726+/-30 Ma. Lowest unit of Kalgoorlie Group. Thickness: 2-5 km. Tholeiitic basalt. Conformably overlain by Silver Lake Member of Kambalda Komatiite. Geological Province: Eastern Goldfields.||||||07-NOV-08
10869|Lunnon Basalt|60627|5|Briefly described|p65 Tb.1|||Of Kalgoorlie Group.||||||
10869|Lunnon Basalt|62108|5|Briefly described|p1409 Tb. 16|Archean|Archean|Of the Kalgoorlie Group. Thin flows of uncontaminated pillowed tholeiites, with thin interflow sediments.  Age: 2720Ma. Thickness: >2000m.Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1417 Fig. 10.||||||07-FEB-11
10869|Lunnon Basalt|62109|5|Briefly described|p1428|Archean|Archean|Pillowed to massive tholeiitic lavas. Age: ca.2720Ma. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton.||||||07-NOV-08
10869|Lunnon Basalt|62110|5|Briefly described|p1442 Fig. 1|Archean|Archean|Age: 2726+/-30Ma. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
10869|Lunnon Basalt|62111|5|Briefly described|p1457|||Of Kambalda Gp. Sequence of thin pillowed and massive tholeiitic metabasaltic flows and intercalated siliceous sedimentary units; rare doleritic sills. Overlain by Kambalda Komatiite Formation.Geol Prov: Kambalda Dome.||||||07-FEB-11
10869|Lunnon Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|NW Kambalda Domain. Kambalda Sequence.|||||Tholeiitic and high MgO basalt.|
10869|Lunnon Basalt|64340|5|Briefly described|p7|||Overlain by Kambalada Komatiite. Max thickness: +1900m.||||||
10869|Lunnon Basalt|64633|6|Mentioned|p4 Fig.3, p6 Fig.4.|||Kalgoorlie Terrane.|c.2715 Ma.|Unit in Kambalda Sequence.||||
10869|Lunnon Basalt|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Kambalda Domain. Tholeiitic and komatiitic basalt flows.||||||11-JUN-15
10869|Lunnon Basalt|65834|6|Mentioned|p7, 44|||Kambalda Domain, Kalgoorlie Terrane.||Kalgoorlie Group.||||
10869|Lunnon Basalt|66854|5|Briefly described|pp943-947.|||Forms part of the core of the Kambalda Anticline. Article proposes a boudinage model and structural-metamorphically-metasomatically emplaced ore-formation rather than magmatic models.||||Overlain by Kambalda Komatiite.||
10869|Lunnon Basalt|66880|5|Briefly described|p7, |Archean|Archean|Correlated with a sill in Woolyeenyer Formation aged 2714 +/- 5 Ma.||Basal unit in Kambalda Sequence.||Is overlain by Kambalda Komatiite.||
10869|Lunnon Basalt|67020|5|Briefly described|p660.|Archean|Archean|Massive Fe-Ni-Cu sulfide bodies occur at contact with Kambalda Komatiite Formation. Typically foliated and/or brecciated approaching contact with Kambalda Komatiite Formation. No metasedimentary rocks observed.||||Is overlain by Kambalda Komatiite Formation.|Pillow basalt.|
10869|Lunnon Basalt|67198|5|Briefly described|p5 Fig.2, p81, p83-84, p94 fig 45, p114|Neoarchean|Neoarchean|See also p112 Fig.48, p118-119, p132-133. Kalgoorlie Terrane. Age derived from volcaniclastics/tuff. Has xenocrystic zircons with >3.4 Ga cores. Forms the footwall to the Kambalda Komatiite. At least 2000m thick, dominated by thin 2-30m flows with a minimum lateral extent of 500km^2. Associated with Ni-sulfide mineralisation. Basalts include tholeiites and all are interpreted to have formed in an aqueous environment during decompression melting of a mantle plume in the subcontinental lithospheric mantle. Imbricated by D1 and D2 faults. Appears as Lunnon Basalts on p86.|2715 Ma|Basal Kambalda Sequence.||Overlain by Silver Lake Member (Kambalda Komatiite). Is intruded by Kambalda Granodiorite.|Fine to medium grained massive basalt, pillowed basalt with well defined rims and radial and subconcentric perlitic fractures, basaltic breccia, sulphidic metasediments and volcaniclastics/tuff.|11-SEP-17
10869|Lunnon Basalt|68110|6|Mentioned|p685|||Discussed in the context of crustal contamination.||||||
10869|Lunnon Basalt|68289|5|Briefly described|p6-p7, p29|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. Suggesed to be either distal to a shield volcano or represents a ponded lava field in an extensional basin. >2000m thick.||||Overlain by the Silver Lake Member (Kambalda Komatiite). Intruded by the Kambalda Granodiorite.|Tholeiitic basalt.|
10869|Lunnon Basalt|69583|5|Briefly described|p37, p39|||Southern Kalgoorlie Terrane. Over 2000m thick.||Kalgoorlie Group.||||
10869|Lunnon Basalt|69586|5|Briefly described|p10|||Kalgoorlie region.||||Equivalent to Never Can Tell Formation.||
10869|Lunnon Basalt|69619|5|Briefly described|p115|||Lowermost unit in Kambalda sequence, Kalgoorlie Terrane.||||Is overlain by Kambalda Komatiite.||
10869|Lunnon Basalt|69631|5|Briefly described|p7, p9, p26|||Kambalda area, Kalgoorlie Terrane. Over 2000m thick.||Kambalda Sequence.||Is overlain by Kambalda Komatiite.||
10869|Lunnon Basalt|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Kambalda Sequence.||Overlain by Kambalda Komatiite.|Basalt.|
10869|Lunnon Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2704 Ma (inferred).|Hannans Subgroup|||Tholeiitic basalt; massive to pillowed; metamorphosed. Mudstone, shale, and minor sandstone as interflow sedimentary rocks; metamorphosed. Basalt to dolerite; interleaved units of fine-grained basalt with coarser layers or zones; metamorphosed.|
10869|Lunnon Basalt|70326|4|Described|p335,360-365|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. Correlable to Hickies Bore Basalt.|c. 2710 Ma|||Overlain by Silver Lake Peridotite and Kambalda Komatiite.|Basalt; massive, pillowed and breccia lithofacies, and can be subdivided into lower Mg-rich and upper Mg-poor components, which are separated by a thin mudstone.|
10869|Lunnon Basalt|70773|5|Briefly described|p18 fig 11, p26, p27|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane.|c. 2710 Ma|Kambalda Sequence||Overlain by the Kambalda Komatiite.|Basalt.|
10869|Lunnon Basalt|70863|6|Mentioned|p9, 11|||Kambalda Dome, Yilgarn Craton. See also Lunnon Basalt Formation (p12).|||||Thick, homogeneous basalt.|
10869|Lunnon Basalt|71148|6|Mentioned|p122, 128, 130-131|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. A plume head. Geochemistry detailed.|2714 +/- 5 Ma (equivalent unit).|Kambalda Sequence.||||
10869|Lunnon Basalt|71166|6|Mentioned|p19|||||||||
10869|Lunnon Basalt|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlain by the Kambalda Komatiite.||
10869|Lunnon 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.|2726-2704 Ma (inferred)|Unit of Hannans Subgroup.|||Basalt; massive to pillowed, to dolerite; interleaved units of fine-grained basalt with coarser layers or zones (probably differentiated flows); metamorphosed; mudstone, shale and minor sandstone as interflow sedimentary rocks; metamorphosed.|
10869|Lunnon Basalt|71308|4|Described|p710-711, p713-714|||Southern Kalgoorlie Terrane. Said to be the "type" stratigraphic unit for the authors' Low-Th Basalts group. Geochemistry discussed in detail.|2710 Ma.|Kambalda Sequence.||Is overlain by Kambalda Komatiite.|Non-vesicular aphyric pillow basalts with massive sheet flows.|
10869|Lunnon Basalt|71309|5|Briefly described|p740 Fig.3, p756|||Eastern Goldfields Superterrane. Crustally-uncontaminated. Referred to as Lunnon basalts on p756. Geochemistry discussed.|2.7 Ga.|||||
10869|Lunnon Basalt|72049|6|Mentioned|p259-p260|||Kalgoorlie Terrane.||Kambalda Sequence||||
10869|Lunnon Basalt|72095|4|Described|p4, p6-26|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Basement to the Kalgoorlie-Kambalda region. Pre-dates regional c.2705 Ma komatiite magmatism. Extensively intruded by mafic and ultramafic sills. Composed of Low-Th basalt (LTB) interlayered with High-Th Siliceous basalt (HTSB) of Barnes et al., 2012.||Base of Hannans Subgroup.||Overlain by Kambalda Komatiite.|Both mafic and some felsic magmatism (appear to be both volcanics and volcaniclastics)|
10869|Lunnon Basalt|72485|6|Mentioned|p3|||||Kambalda Sequence.||||
10869|Lunnon Basalt|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
10869|Lunnon Basalt|73391|5|Briefly described|p19, 279, Appendices.|||Cowden and Roberts (1990). Regional stratigraphic correlation chart of other workers. Kambalda Domain, Kalgoorlie Terrane. >2000m thick.||Lower Basalt.||Equivalent to Woolyeener Formation.|Pillowed to massive tholeiitic basalts, minor gabbro, rare interflow sedimentary rocks.|
10869|Lunnon Basalt|73596|6|Mentioned|p1160, 1162|||Appears as Lunnon/Missouri Basalt.||Hannans Subgroup.||||
10871|Lupton Formation|22716|6|Mentioned|table4,p231|Neoproterozoic III|Neoproterozoic III|Age: 610Ma||||||
10871|Lupton Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin.||||||27-MAY-09
10871|Lupton Formation|22901|3|Fully described|74|||Geol province Officer Basin.||||||26-AUG-08
10871|Lupton Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
10871|Lupton Formation|23571|4|Described|p11|||Geological Province: Officer Basin. Underlying Unit: Townsend Quartzite and Lefroy Formation (both unconformable).||||||
10871|Lupton Formation|24161|4|Described|p9 Fig.6, p13|||Unconformably overlies the Steptoe Formation. Unconformably overlain by the Table Hill Volcanics. Wahlgu Formation has been proposed to replace the name Lupton Formation for the Supersequence 3 glacial deposits. Geological Province: Officer Basin.||||||30-NOV-06
10871|Lupton Formation|24390|5|Briefly described|p12|||Geological Province: Officer Basin.  See also p11 Fig. 6.||||||
10871|Lupton Formation|41751|6|Mentioned|p8|||||||||
10871|Lupton Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~600Ma.  Geological Province: Officer Basin.||||||
10871|Lupton Formation|50205|5|Briefly described|p59 Fig.1|Fortunian|Neoproterozoic|Of Officer Basin.||||||
10871|Lupton Formation|60118|6|Mentioned|p30|||Contains halite beds <10m thick. Geological Province: Officer Basin.||||||
10871|Lupton Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
10871|Lupton Formation|61272|5|Briefly described|p120 Fig.1|||Unconformably overlies the Kanpa Formation. Unconformably overlain by the ?McFadden Formation. See also p123 Fig.4||||||27-MAY-06
10871|Lupton Formation|61732|3|Fully described|p58, p85|Cryogenian|Cryogenian|Comprises a lower conglomeratic diamictite and upper interbedded conglomerate, with cross-bedded sandstone and minor siltstone. Disconformable on Lefroy Fm. Max. thickness: >250m. Geological Prov: Officer Basin. See also "Lupton Fm".||||||07-FEB-11
10871|Lupton Formation|62453|3|Fully described|p5 Fig. 3, 45|Ediacaran|Ediacaran|Geological Province: Officer Basin. Unconformably overlies: Lefroy Formation. Diamictite, sandstone and siltstone, conglomerate.||||||
10871|Lupton Formation|62987|6|Mentioned|p30|||Previously contained the Wahlgu Formation.||||||
10871|Lupton Formation|64325|5|Briefly described|p82 Fig. 2||Late NeoproterozoicEarly Cambrian|Age: ~545Ma. Geological Province: western Officer Basin. Sandstone unit.||||||26-AUG-08
10871|Lupton Formation|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Massive pebble to boulder conglomerate (tillite) and medium- to thick-bedded sandstone; minor siltstone.||||||09-DEC-08
10871|Lupton Formation|64793|6|Mentioned|p286 Fig.5, p291 fig 8|Neoproterozoic|Neoproterozoic|Of central Officer Basin.|||||Diamictite, cap dolomite, sandstone.|
10871|Lupton Formation|64796|6|Mentioned|p200 Fig.10|Neoproterozoic|Neoproterozoic|||||||
10871|Lupton Formation|64970|5|Briefly described|p718, p719 Fig. 2,  p 721 Fig. 5|Neoproterozoic|Neoproterozoic|Tillites and fluvio-glacial deposits. Geological Province: Officer Basin.||||||27-MAY-09
10871|Lupton Formation|65102|4|Described|p363, 366-7, 368, 371, Fig4-38, 4-4|Neoproterozoic|Neoproterozoic|Paterson Orogen (SE) and Officer Basin. Several hundred m; tillite, cross-bedded sandstone; minor siltstone; glacial, marine to fluvial; disconformable on Lefroy Formation; type section at Lupton Hills, 26deg 31min S, 128deg 01min E; unfossiliferous; Sturtian/Marinoan from stratigraphic correlation.||||||
10871|Lupton Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||||||
10871|Lupton Formation|65410|5|Briefly described|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin.|||||Tillite.|
10871|Lupton Formation|65416|5|Briefly described|p137, p141, p145, p146.|Neoproterozoic|Neoproterozoic|Officer Basin. Could be included in Supersequence LP2 or LP3. Outcrops south of Musgrave Complex.||||Unconformably overlies Lefroy Formation.|Massive conglomerate with scattered boulders, and sandstone with interbeds of siltstone and diamictite.|
10871|Lupton Formation|67195|5|Briefly described|p9 fig 5, p10, p19 tbl 1, p47|Cambrian|Neoproterozoic|Western Officer Basin.||||Unconformably overlain by Table Hill Volcanics, Unconformably overlies Steptoe Formation|Sandstone.|
10871|Lupton Formation|68270|4|Described|p678,682-684,687-688|Cryogenian|Cryogenian|Western Officer Basin. Type section is in Lupton Hills; lat, 26'32.5'S, long. 128'2.6"E. Up to 250m thick in type section (Lupton Hills). ?Glacial in part. Crops out in the western Officer Basin south of the Musgrave Province. Related to Elatina glaciation. Possible lateral equivalent of Wahlgu and Boondawari Formations.||||Underlain unconformably by Townsend Quartzite and Lefroy Formation.|Diamictite, conglomerate, sandstone and mudstone, with rare striated and faceted clasts.|03-JUL-19
10871|Lupton Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
10871|Lupton Formation|69029|6|Mentioned|p329|Cambrian|Neoproterozoic|Of Officer Basin.||||Overlain unconformably by Table Hill Volcanics. Underlain unconformably by Steptoe Formation.||
10871|Lupton Formation|69091|6|Mentioned|p43, p106 Fig.5.7a, see comments|||Western Officer Basin. A ?glacigene unit which overlies Townsend Quartzite in outcrop, and may have been mismapped as Permian in some areas, based on outcrop trends and relationships. See also p107 Fig.5.8a, p109 Fig.5.10.||||Equivalent to Pirrilyungku Formation.||07-OCT-14
10871|Lupton Formation|69153|6|Mentioned|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Massive pebble to boulder conglomerate (tillite) and medium- to thick-bedded sandstone; minor siltstone; glacial|
10871|Lupton Formation|70137|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||||Overlies Buldya Group.|Diamictite and sandstone.|
10871|Lupton Formation|70634|4|Described|100k_geologyp_lut,csv|Cryogenian|Cryogenian||635 Ma- 850 Ma (Inferred)||||Diamictite and sandstone.|
10871|Lupton Formation|70793|4|Described|GEOL_LUT_CSV files|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 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.|720-635 Ma (inferred)||||Diamictite and sandstone|
10871|Lupton Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 2, Centralian Superbasin.||||||20-APR-20
10871|Lupton Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tillite, sandstone, conglomerate|
10871|Lupton Formation|71268|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|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, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|720-635 Ma (inferred)||||Diamictite and sandstone|
10871|Lupton Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Ediacaran|Officer Basin.||||Overlies the Hussar Formation.|Diamictite.|
10871|Lupton Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Cryogenian|Officer Basin (Phase 1).|||||Diamictite and sandstone.|
10906|M3 Formation|42677|6|Mentioned|p19|||||||||
10920|MacDougall Formation|30390|4|Described|p54|||||||||
10920|MacDougall Formation|36551|6|Mentioned|Table 31|||||||||
10920|MacDougall Formation|65135|5|Briefly described|p16|||Conglomerates. Formerly part of the Tollu Group. Redefined in this paper as part of the Kunmarnara Group. Overlain by Mummawarrawarra Basalt. Mainly restricted to outcrops south of the poorly exposed southern limb of a syncline south of the Blackstone intrusion.||||||
10920|MacDougall Formation|65256|5|Briefly described|p13, 14, 38|||Basal unit of the Tollu Group. Quartzite, sandstone and rounded pebble conglomerate. Correlated with Karukali Quartzite; conformably underlies Mummawarrawarra Basalt. See also MacDougall Bluff Formation, Fig. 10.||||||25-MAR-15
10920|MacDougall Formation|65833|5|Briefly described|p16|Stenian|Stenian|Basal unit of Kunmarnara Group (and formerly of the Tollu Group). Overlain by Mummawarrawarra Basalt. Sandstones, pebbly sandstones and conglomerates.||||||
10920|MacDougall Formation|65906|6|Mentioned|p20|Mesoproterozoic|Mesoproterozoic|Maximum depositional age: 1172 +/- 8 Ma (detrital zircon).  Lowest unit of the Kunmarnara Group.||||||
10920|MacDougall Formation|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Unit in Kunmarnara Group. Strongly-foliated quartz-pebble conglomerate, feldspathic sandstone, muscovite quartzite, and phyllite; metamorphosed; locally garnetiferous near mafic intrusions.||||||
10920|MacDougall Formation|67128|4|Described|p5 Fig.3, p11, p15, p17-19, p32|||Western Musgrave Province. Typically forms low sandy outcrops and linear ridges in dune country; elsewhere ferricrete mounds. Detrital zircon maximum deposition age.|c.1170 Ma.|Kunmarnara Group.||Unconformably overlies Wankanki Supersuite and Wirku Metamorphics. Is overlain by Mummawarrawarra Basalt.|Fine- to coarse-grained, muddy to arkosic, poorly sorted basal and pebbly sandstones, and matrix-supported conglomerates with an overwhelming majority of vein quartz pebbles.|
10920|MacDougall Formation|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Written as MACDOUGALL; see also Macdougall Formation.||Unit in Kunmarnara Group.|||Quartz pebble conglomerate and sandstone; medium- to coarse-grained sandstone; locally pebble beds and rare quartz-pebble conglomerate.|11-APR-12
10920|MacDougall Formation|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Kunmarnara Group.|||Quartz-pebble conglomerate and sandstone; locally medium- to coarse-grained, foliated, or mylonitic; feldspathic metasandstone; muscovite quartzite; phyllite; locally garnetiferous near mafic intrusions.|
10920|MacDougall Formation|67375|3|Fully described|p38 Table 1, p39, p40, pp216-230.|Mesoproterozoic|Mesoproterozoic|Formerly the basal unit in Tollu Group. Now reassigned to Kunmarnara Group. Fluvial sediments. Contains detrital zircons aged 1172 +/- 8 Ma, giving the maximum age for this unit and the Kunmarnara Group. Forms low outcrops and linear ridges in dune country, and sparolitic or limonitic ferricrete mounds in lower lying areas. Best exposed in the Mount Blyth area.|1172 +/- 8 Ma - 1076 +/- 7 Ma (Evins et al. 2010).|Unit in Kunmarnara Group.||Unconformably overlies Wankanki Supersuite and Wirku Metamorphics. Is intruded by oldest Giles Suite intrusions. Is overlain conformably by Mummawarrawarra Basalt.|Poorly-sorted, muddy to arkosic sandstones, pebbly arkose, pebble beds and matrix-supported quartz-pebble conglomerates; pebbles mostly of vein quartz; typically deformed and metamorphosed to form a muscovite-bearing quartzite; locally garnetiferous|
10920|MacDougall Formation|67553|4|Described|p39-40,42,84-85|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).||Unit of Kunmarnara Group.||Lower unit of Kunmarnara Group. Overlain by Mummawarrawarra Basalt.|Interbedded coarsegrained arkosic sandstone, pebbly arkose, pebble beds, and matrix-supported conglomerate.|
10920|MacDougall Formation|68100|5|Briefly described|p3, 5, 7, 8, 27, 28, 30|Mesoproterozoic|Mesoproterozoic|Basal unit of the Ngaanyatjarra Rift succession (Evins et al., 2010). Detrital zircon age spectra dominated by 1220-1155 Ma Pitjantjatjara Supersuite sources.|c. 1175 Ma|Kunmarnara Group||Disconformably overlies gneisses of Wirku Matamorphics.|Non-metamorphosed sandstones and conglomerates. Pebbly sandstone.|19-JAN-17
10920|MacDougall Formation|68995|5|Briefly described|p6, p48|||||Kunmarnara Group|||Quartz sandstones, pebbly sandstones and conglomerates.|
10920|MacDougall Formation|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin. 7 facies are mapped separately.|c. 1078 Ma|Of the Kunmarnara Group.|||Metamorphosed arkose; granofels; quartzite; schist; metaconglomerate and metasandstone.|04-APR-14
10920|MacDougall Formation|69091|5|Briefly described|p70, p80|||Basal unit of Bentley Supergroup.||Basal Kunmarnara Group.||Equivalent to Karukali Quartzite (Tjauwata Group).|Quartz sandstones, pebbly sandstones and conglomerates.|26-SEP-14
10920|MacDougall Formation|69153|5|Briefly described|GEOL_LUT_CSV files; GEOCHRON files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Several detrital zircon ages given.|1106+/-39 Ma (max depositional age)|lowermost unit of Kunmarnara Group||is overlain by Mummawarrawarra Basalt|Quartz-pebble conglomerate and medium- to coarse-grained sandstone; mylonitic and strongly foliated quartz-pebble metaconglomerate, feldspathic metasandstone, muscovite quartzite, and phyllite; locally garnetiferous near mafic intrusions|15-AUG-18
10920|MacDougall Formation|69436|5|Briefly described|p21:14|||Of Daniels (1974), who assigned it to the Tollu Group. Now assigned to the Kunmarnara Group.||Kunmarnara Group.||Lateral equivalent of the Karukali Quartzite.|Sandstones, pebbly sandstones and conglomerates.|12-JUL-16
10920|MacDougall Formation|69729|5|Briefly described|p79, p86|Neoproterozoic|Neoproterozoic|Ar-Ar muscovite plateau age (metamorphism).|c.623 Ma.|Kunmarnara Group.||Equivalent to the Karukali Quartzite.|Includes greenschist facies micaceous quartzite.|
10920|MacDougall Formation|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The three facies are mapped separately.|>1078 Ma.|Kunmarnara Group.|||Medium- to coarse-grained quartzite, locally with muscovite and garnet (section only); or interlayered with muscovite schist, local quartz-pebble conglomerate; muscovite(-garnet-kyanite) granofels, metamorphosed arkose, quartzofeldspathic gneiss.|
10920|MacDougall Formation|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c. 1078 Ma|Kunmarnara Group|||Conglomerate and sandstone; metamorphosed siliclastic rocks; granofels; quartzite and schist; paragneiss.|
10920|MacDougall Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP date from sample (185414.2.pdf)|1075 Ma - 1085 Ma (Inferred) 1086 Ma (SHRIMP)|Kunmarnara Group||Conformably overlain by Mummawarrawarra Basalt|Quartz-pebble metaconglomerate, feldspathic metasandstone, muscovite quartzite, phyllite, quartz-pebble conglomerate and sandstone.Metamorphosed arkose; granofels interlayered with medium-coarse grained quartzite and schist.|
10920|MacDougall Formation|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Seven facies are mapped separately.|c.1078 Ma.|Kunmarnara Group.|||Metaconglomerate, metasandstone, quartzite, phyllite, psammitic gneiss, amphibolite, metamorphosed arkose, interlayered quartzite and schist, muscovite granofels.|
10920|MacDougall 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). Characterised by coarse-grained fluvial sedimentation with basaltic andesites and andesite with high-K intraplate geochemistry. Metamorphosed to granulite facies. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 185414 (quartzite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1153+\-9 Ma for the sedimentary protolith, and a muscovite crystallisation age (Ar-Ar plateau) of 623+\-5 Ma. Sample GSWA 190233 (phyllite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1172+\-8 Ma for the sedimentary protolith. Sample GSWA 190292 (metasandstone) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) maximum depositional age of 1176+\-7 Ma for the sandstone. Sample GSWA 194420 (feldspathic sandstone) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) maximum depositional age of 1173+\-6 Ma for the sandstone. Sample GSWA 194806 (metasandstone) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) maximum depositional age of 1179+\-5 Ma for the sandstone. Sample GSWA 201307 (metasandstone) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1172+\-10 Ma for the sandstone. Sample GSWA 201311 (metasandstone) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1180+\-8 Ma for the sandstone. Sample GSWA 205194 (psammitic) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1190+\-12 Ma for the sandstone. 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.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.||Lowermost unit of Kunmarnara Group.|Interlayered quartzite and muscovite(-garnet-kyanite) schist, local quartz pebble conglomerate, sandstone, metamorphosed arkose and quartzite, metaconglomerate, psammitic gneiss and granofels.|
10920|MacDougall Formation|70831|5|Briefly described|p1-p2, p4-p6, p9|Stenian|Stenian|Musgrave Province. Deposited during the Giles Event. Geophysical response and zircon age spectra are discussed.  Beds typically range from 10 to 50cm thick. Interpreted as a fluvial sandstone and pebble conglomerate metamorphosed under amphibolite-facies conditions. See also  p11, p13, p17-p18, p22-p26.|c. 1085-1040 Ma|Kunmarnara Group||Overlain by the Mummawarrawarra Basalt.|Interbedded, medium- to coarse-grained quartzite, muscovite-garnet-magnetite schist and local quartz-pebble conglomerate.|
10920|MacDougall Formation|71170|5|Briefly described|p112|||Metamorphism is dated at ca. 623 Ma by Ar/Ar (Kirkland et al, 2013a) and at ca. 631 Ma by U-Pb (Kirkland et al, 2014).||||||
10920|MacDougall Formation|71210|5|Briefly described|p8, p136|||||Kunmarnara Group||Equivalent to the Karukali Quartzite.|Deformed sandstones and conglomerate.|
10920|MacDougall Formation|71211|5|Briefly described|p233|||||Kunmarnara Group|||Basal sandstones, pebbly sandstones and conglomerates.|
10920|MacDougall 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 185414 (muscovite in quartzite) yielded an Ar-Ar plateau date at 623+\-5 Ma, interpreted to be time of muscovite crystallisation; and a weighted mean 207Pb/206Pb age of 1153+\-9 Ma, interpreted as maximum depositional age for sedimentary protolith. Sample GSWA 190223 (phyllite) yielded a weighted mean 207Pb/206Pb age of 1172+\-8 Ma, interpreted to be maximum depositional age. Sample GSWA 190292 (metasandstone) yielded a concordia age of 1176+\-7 Ma, interpreted as maximum depositional age. Sample GSWA 194420 (poorly sorted arkose) yielded a concordia age of 1173+\-6 Ma, interpreted as maximum depositional age of the arkose. Sample GSWA 194806 (arkosic metasandstone) yielded a weighted mean 207Pb/206Pb age of 1179+\-5 Ma, interpreted as maximum depositional age of sedimentary precursor. Samples GSWA 201307 and 201311 (metasandstone) yielded weighted mean 207Pb/206Pb ages of 1172+\-10 and 1180+\-8 Ma, interpreted as maximum depositional ages of sandstone samples. Sample GSWA 205194 (psammitic gneiss) yielded a weighted mean 207Pb/206Pb date of 1190+\-12 Ma, interpreted as maximum depositional age of the sandstone protolith. Sample GSWA 208414 (quartzite) yielded a weighted mean 207Pb/206Pb date of 1179+\-13 Ma, interpreted as maximum depositional age of the sandstone protolith; and metamorphism at 631+\-12 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, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1085-1075 Ma (inferred)|Unit of Kunmarnara Group.||Lowermost unit of Kumarnara Group. Overlain by Mummawarrawarra Basalt. Equivalent to Karukali Quartzite.|Interlayered quartzite and muscovite(-garnet-kyanite) schist and local quartz-pebble conglomerate, mylonitic; sandstone; metamorphosed; psammitic gneiss and quartzofeldspathic gneiss.|
10920|MacDougall Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Kunmarnara Group|||Quartz-pebble conglomerate, sandstone. Metamorphosed arkose, quartzite. Psammitic, garnet-bearing granofels; local bedding-parallel amphibolite. Psammitic gneiss; biotite-garnet(-magnetite) quartzofeldspathic gneiss; migmatitic; local amphibolite.|
10920|MacDougall Formation|72094|4|Described|p4, p9, p11, p12, p14, 17|Stenian|Stenian|Musgrave Province. Outcrops in Mitika Area. U-Pb detrital zircon geochronology yield ages of 1650-1550 Ma (broad peaks), c. 1415 Ma (minor peak) and 1220-1150 Ma (dominant peak). Maximum depositional age is 1177+/-4 Ma (Quinten de Gromard et al., 2016b), although max dep ages range down to 1153+/-9 Ma; minimum depositional age constrained by 1078+\-4 Ma syenetic volcanic rock of Kunmarnara Group and 1076+\-7 Ma leucogabbro intrusion into Kunmarnara Group (Kirkland et al., 2011b, 2012b). Summary table of zircon geochronology on p9 Table 2.|Max dep age is 1177+/-4 Ma|Unit of Kunmarnara Group||Underlain by Mummawarrawarra Basalt. Likely time- and lateral equivalent to the Karukali Quartzite.|Interbedded quartzite, quartzofeldspathic metasandstone and quartz-pebble metaconglomerate.|
10920|MacDougall Formation|73437|6|Mentioned|p153|||Deposited at the onset of the Giles Event.||Kunmarnara Group|||Siliciclastic sediments.|
10925|MacLeod Member|22689|6|Mentioned|Fig. 1 p138|||Of Marra Mamba Iron Formation.||||||
10925|MacLeod Member|23126|4|Described|p382|||||||||
10925|MacLeod Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Marra Mamba Iron Formation. Overlies Namuldi Member. Overlain by Mount Newman Member. Shale. Geological Province: Hamersley Basin.||||||07-NOV-08
10925|MacLeod Member|42112|5|Briefly described|p8|||Reserved as MacLeod||||||
10925|MacLeod Member|42190|6|Mentioned|Fig.3 p273|||||||||27-OCT-15
10925|MacLeod Member|42471|5|Briefly described|p7|||of Marra Mamba Iron Formation.||||||
10925|MacLeod Member|42495|5|Briefly described|p35|||||||||
10925|MacLeod Member|42744|4|Described|p4|||Of Marra Mamba Iron Formation.||||||
10925|MacLeod Member|43063|3|Fully described|p54|||Of Marra Mamba Iron Formation.||||||08-APR-09
10925|MacLeod Member|43119|5|Briefly described|p9|||of Marra Mamba Iron Formation||||||
10925|MacLeod Member|43210|5|Briefly described|Table 1 p3,p4.|||of Marra Mamba Iron Formation.||||||
10925|MacLeod Member|43290|5|Briefly described|p6||Archean|of Marra Mamba Iron Formation.||||||07-NOV-08
10925|MacLeod Member|60706|5|Briefly described|p623 Fig.2||Archean|Of the Marra Mamba Iron Formation (Hamersley Group). Geological Province: Hamersley Basin.||||||07-NOV-08
10925|MacLeod Member|62129|3|Fully described|p9|Archaean|Archaean|Of Marra Mamba Iron Formation. Underlain by Nummuldi Member. Thickness: 45m. Geological Province: Hamersley Basin.||||||07-FEB-11
10925|MacLeod Member|63153|6|Mentioned|p1359-1375.|||Appears as McLeod in Fig.2. Shows numerous sedimentary structures characteristic of current deposition. Magnetite-silicate BIF is abundant.||Unit in Marra Mamba Iron Formation.||Overlies Nammuldi Member. Is overlain by Mount Newman Member.|Includes low-grade (50-60 wt % Fe) iron ore deposits, mainly limonite and goethite, with high alumina and silica from interbedded clay.|
10925|MacLeod Member|64384|5|Briefly described|p35 Tb. 6|||Of Marra Mamba Iron Formation (Hamersley Group). Overlies Nammuldi Member; underlies Mount Newman Member. Geological province: Hamersley Basin. Shale with thin BIF interbeds; chert.||||||07-FEB-11
10925|MacLeod Member|65683|4|Described|p799, p800, p801 Fig2, p802, p805|||Of Marra Mamba Iron Formation. Underlies Mount Newman Member; overlies Nammuldi Member. Minimum apparent thickness is 42 m in weathered material. Iron formation.||||||08-MAR-12
10925|MacLeod Member|67056|6|Mentioned|p419 Fig.2. |||||Unit in Marra Mamba Iron Formation.||Overlies Nammuldi Member. Is overlain by Mount Newman Member.||
10925|MacLeod Member|67130|5|Briefly described|p3 fig 2|||||Marra Mamba Iron Formation||Overlies Nammuldi Member, overlain by Mount Newman Member|Shale.|
10925|MacLeod Member|67201|5|Briefly described|p34 Fig.18|||||Marra Mamba Iron Formation||||
10925|MacLeod Member|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean|Approximately 75 m thick.|c. 2597 Ma|Of the Marra Mamba iron formation.|||Shaly banded iron formation.|
10925|MacLeod Member|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.||Of Marra Mamba Iron Formation.||Overlies Nammuldi Member, overlain by Mount Newman Member.|Shale.|
10925|MacLeod Member|68280|6|Mentioned|p5|||||Marra Mamba Iron Formation|||Shale.|
10925|MacLeod Member|69538|6|Mentioned|p517 Fig.3, p529 Fig.9, p583-585|||||Unit in Marra Mamba Iron Formation.||||
10925|MacLeod Member|71808|4|Described|vi, p9, p11, p15, p19, p39, p53|||Hamersley Province. 74m thick in the type section, includes two informal beds the Potato Bed and Football Chert. Previously the Middle Shale Member.See also p85, p95, p117, p127, p129, p150, p153, p169, p172-p173, p223, p225, p240.||Marra Mamba Iron Formation||Faulted over the Jeerinah Formation.|Chert and two minor thinner but prominent podded units.|
10925|MacLeod Member|73022|6|Mentioned|p3 Fig.2|||||Marra Mamba Iron Formation||Overlies the Nammuldi Member, underlies the Mount Newman Member.|Shale, minor Fe-chert and banded iron formation.|
10925|MacLeod Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
10925|MacLeod Member|73538|6|Mentioned|p4|||||Marra Mamba Iron Formation||Underlain by Nammudi Member. Overlain by Mount Newman member.|Mudstone/siltstone.|
10938|Machells Pyramid Lamproite|41158|5|Briefly described|Table 43|||||||||
10979|Madeline Formation|23279|6|Mentioned|p16|||||||||
10979|Madeline Formation|23815|4|Described|p285|Artinskian|Artinskian|Geological Province: Byro Sub-basin. Of the Newman Subgroup. Overlying unit: Bogadi Greywacke (confomable). Underlying unit: Keogh Formation (conformable). Max. thickness: 152 m. Richly fossiliferous.||||||
10979|Madeline Formation|30550|6|Mentioned|p94|||Fauna||||||
10979|Madeline Formation|32648|6|Mentioned|p32|||Byro Gp.||||||
10979|Madeline Formation|33594|6|Mentioned|p37|||||||||
10979|Madeline Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
10979|Madeline Formation|34532|6|Mentioned|p221|||See also P222,224,226. L.Perm.||||||
10979|Madeline Formation|34570|6|Mentioned|p114|||||||||
10979|Madeline Formation|36020|6|Mentioned|p392|||||||||
10979|Madeline Formation|36208|6|Mentioned|p253|||||||||
10979|Madeline Formation|36293|6|Mentioned|p117|||||||||
10979|Madeline Formation|36387|6|Mentioned|p186|||||||||
10979|Madeline Formation|36890|3|Fully described|p285|||||||||
10979|Madeline Formation|37295|6|Mentioned|p54|||See also Table 2.||||||
10979|Madeline Formation|37549|6|Mentioned|p110|||||||||
10979|Madeline Formation|39223|6|Mentioned|p242|||||||||
10979|Madeline Formation|41044|6|Mentioned|p134|||||||||
10979|Madeline Formation|41049|6|Mentioned|p43|||||||||
10979|Madeline Formation|41053|6|Mentioned|Fig.2|||||||||
10979|Madeline Formation|41071|6|Mentioned|p20|||||||||
10979|Madeline Formation|41100|6|Mentioned|Fig.9|||||||||
10979|Madeline Formation|41315|6|Mentioned|p155|||||||||
10979|Madeline Formation|42462|6|Mentioned|p56|||See also p60.||||||
10979|Madeline Formation|42654|6|Mentioned|p4|||||||||
10979|Madeline Formation|42994|6|Mentioned|p33|||||||||
10979|Madeline Formation|43015|5|Briefly described|Table 1,p319|||||||||
10979|Madeline Formation|43495|6|Mentioned|13||Artinskian|||||||
10979|Madeline Formation|44040|14|Not recorded|p43|||||||||
10979|Madeline Formation|44217|14|Not recorded|Fig.3|||||||||
10979|Madeline Formation|44237|14|Not recorded|p.201|||||||||
10979|Madeline Formation|44344|14|Not recorded|p.12|||Equiv. of Coyrie Fm. (G50-1).||||||
10979|Madeline Formation|44994|6|Mentioned|Fig.7|||Permian. Correlation||||||
10979|Madeline Formation|45001|14|Not recorded|p146|||Of Byro Group||||||
10979|Madeline Formation|45015|5|Briefly described|map|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group). Geological Province: Carnarvon Basin.||||||31-MAY-06
10979|Madeline Formation|45016|2|Defined|p.145-150||Artinskian|Tb, p.77,99-102,105,107,115-6,118,121,124,126,132,151-2. (G50-6).||||||
10979|Madeline Formation|48831|14|Not recorded|p.25,35|||||||||
10979|Madeline Formation|48848|14|Not recorded|p.65|||||||||
10979|Madeline Formation|48885|14|Not recorded|p.2,5,9-11,13||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6). pl.2.||||||
10979|Madeline Formation|49644|5|Briefly described|Table|||||||||
10979|Madeline Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group).||||||21-MAR-06
10979|Madeline Formation|64974|6|Mentioned|p147 Fig. 5|Artinskian|Artinskian|Geological Province: Carnarvon Basin.||||||24-JUN-09
10979|Madeline Formation|67195|5|Briefly described|Appendix 3|||Carnarvon Basin.|||||Dark grey siltstone, claystone; rare fossiliferous (graptolite?).|
10979|Madeline Formation|67200|6|Mentioned|p18 table 1, p49, p54, app 2 p11|||Thermal conductivity of 1.53 W/mK||Byro Group|||Siltstone, claystone, rare fossiliferous (graptolite?)|
10986|Madoonga beds|40356|6|Mentioned|p7|||Informal nomenclature||||||
10987|Madura Formation|22663|5|Briefly described|S97-1 and 2 p3||Early Cretaceous|||||||01-MAR-10
10987|Madura Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
10987|Madura Formation|23989|5|Briefly described|p51|Cretaceous|Cretaceous|Geological Province: Officer Basin||||||03-MAR-10
10987|Madura Formation|24057|5|Briefly described|p97|Cretaceous|Cretaceous|Geological Basin: Eucla Basin.||||||
10987|Madura Formation|30012|4|Described|Table 1|||||||||
10987|Madura Formation|30268|6|Mentioned|p44|||||||||
10987|Madura Formation|30563|4|Described|p11|||Stratigraphic table on p7.||||||07-OCT-20
10987|Madura Formation|30564|5|Briefly described|p11|||||||||
10987|Madura Formation|30945|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|30975|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|31153|6|Mentioned|p111|||Refers bivalves of Eucla Basin.||||||
10987|Madura Formation|31562|6|Mentioned|p11|||Refers Lowry (1970)||||||
10987|Madura Formation|31902|4|Described|Table 1|||Fig.1||||||
10987|Madura Formation|31903|6|Mentioned|Map legend|Cretaceous|Cretaceous|Section only||||||
10987|Madura Formation|31904|4|Described|p7|||Table 1. Refers Fairbridge (1953), McWhae et al. (1958)||||||
10987|Madura Formation|31906|4|Described|p7|||Cretaceous. Table 1||||||
10987|Madura Formation|31907|4|Described|Table 1|||U. & L. Cret.||||||
10987|Madura Formation|31908|4|Described|Table 1|||U. & L. Cret.||||||
10987|Madura Formation|31909|3|Fully described|p7|||Formerly "Madura Shale". Type section||||||
10987|Madura Formation|31915|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|32552|2|Defined|p10|Cretaceous|Cretaceous|See also P37, 47, 49, 50-56 etc.||||||
10987|Madura Formation|32648|6|Mentioned|p32|||Cretaceous.||||||
10987|Madura Formation|32747|6|Mentioned|p365|||Comparison of sediments||||||
10987|Madura Formation|33586|4|Described|Table 1|||See also P13.||||||
10987|Madura Formation|33589|5|Briefly described|p10|||Cret.||||||
10987|Madura Formation|33592|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|33595|4|Described|Table 1|||||||||
10987|Madura Formation|34192|6|Mentioned|Map legend|Cenomanian|Albian|Cenomanian - Aptian||||||
10987|Madura Formation|34194|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
10987|Madura Formation|34742|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
10987|Madura Formation|35496|4|Described|Table 1|||Also on p20.||||||07-OCT-20
10987|Madura Formation|36257|6|Mentioned|Table 2.1|||||||||
10987|Madura Formation|36701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10987|Madura Formation|36890|3|Fully described|p412|||Formerly Madura Shale||||||
10987|Madura Formation|36902|6|Mentioned|p24|||||||||
10987|Madura Formation|36915|6|Mentioned|Fig.7|||||||||
10987|Madura Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
10987|Madura Formation|38482|6|Mentioned|p24|||See also Table 11.||||||
10987|Madura Formation|39211|5|Briefly described|p69|||See Fig. 44||||||
10987|Madura Formation|39923|6|Mentioned|p354|||||||||
10987|Madura Formation|40992|6|Mentioned|Fig.23|||||||||
10987|Madura Formation|41751|3|Fully described|p1|||||||||
10987|Madura Formation|42108|4|Described|p319|||||||||
10987|Madura Formation|42315|6|Mentioned|p2|Aptian|Neocomian|||||||
10987|Madura Formation|42545|3|Fully described|p14|Aptian|Hauterivian|||||||
10987|Madura Formation|42959|5|Briefly described|p58 Fig.3|||||||||
10987|Madura Formation|43026|5|Briefly described|Table 1,p586|||||||||
10987|Madura Formation|43252|5|Briefly described|p163|||||||||
10987|Madura Formation|43498|6|Mentioned|8|Santonian|Neocomian|||||||
10987|Madura Formation|43814|6|Mentioned|Fig.3,p115|||||||||
10987|Madura Formation|44133|4|Described|p134|Aptian|Barremian|Previously known as 'Madura Shale'. Conformably overlies: Loongana Formation. Underlies disconformably the Hampton Sandstone. Overlain by Toondi Formation. Thickness: 474m.||||||
10987|Madura Formation|44145|4|Described|p549 fig 4-190, p553-4, p551, 559, 552|Aptian|Barremian|Eucla Basin. Base is time transgressive. Barremian or older onshore; latest Barremian offshore. Age from sparse flora & fauna. Type section in Transcontinental Railway 1 bore, Madura.||||Conformably overlies Loongana Sandstone. Grades northwards into Samuel Formation and Bejah Claystone.|Carbonaceous sandstone, siltstone, claystone and shale: commonly pyritic.|
10987|Madura Formation|44412|14|Not recorded|map legend||Cretaceous|Cret.||||||
10987|Madura Formation|45149|2|Defined|p60|Early Cretaceous|Early Cretaceous|See also Table 1 and p15.||||||07-OCT-20
10987|Madura Formation|45168|6|Mentioned|p6|||See also Table 1||||||
10987|Madura Formation|49060|5|Briefly described|Fig.15|||See also Fig. 5||||||
10987|Madura Formation|61197|5|Briefly described|p473, p475|Middle Cretaceous|Early Cretaceous|Eucla Basin. Continental to low-energy marine deposits. 0-120m thick.|||||Silt, clay/shale, carbonaceous sand; pyritic.|
10987|Madura Formation|61630|6|Mentioned|p555 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eyre Sub-basin.||||||07-APR-09
10987|Madura Formation|62640|6|Mentioned|p73 Fig.7. |||||||Is overlain by Wilson Bluff Limestone.||
10987|Madura Formation|64580|4|Described|map legend||Early Cretaceous|Cross-bedded feldspathic sandstone, locally conglomeratic, carbonaceous sandstone; glauconitic sandstone, siltstone, claystone and shale; commonly pyritic.||||||09-DEC-08
10987|Madura Formation|65102|4|Described|p.366,369,375, Figs.4-41,4-53, Table4-15|Early Cretaceous|Early Cretaceous|Officer Basin. 6-951m; quartzose sandstone, glauconitic greensand & claystone; marine, mostly low energy; conformable on Loongana Sandstone; type section at Naries Point, 28deg 50min S, 124deg 52min E; contains sponges, trace fossils; Neocomian.||||||16-JUL-13
10987|Madura Formation|68715|6|Mentioned|p30 Fig.5|Barremian|Barremian|Bight Basin.||||||
10987|Madura Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Albian|Barremian|Eyre Sub-basin.||||Overlies the Loongana Formation. Overlain by the Ceduna Formation.|Shale.|
10987|Madura Formation|69598|5|Briefly described|p9, p11|Cretaceous|Cretaceous|Central Eucla Basin. Up to 274m thick. Contains potential seal lithologies.|||||Fluvial to marine claystones, carbonaceous mudstones, siltstones and sandstone.|
10987|Madura Formation|69632|5|Briefly described|p21 Tb.6, p26, p30, p32|Cretaceous|Cretaceous|Gunbarrel, Eucla Basins. Average shear-wave velocities tabulated. Palynomorphs indicate marine sedimentation for all but the base.||Bight Basin Group.||Overlies Loongana Formation.|Glauconitic, carbonaceous, pyritic sandstone, siltstone, grey claystone/shale, mudstone.|
10987|Madura Formation|69648|4|Described|p20-21, p38, map legend|Early Cretaceous|Early Cretaceous|Of Bight Basin margin. Occurs in drillholes. Maximum local thickness of 43 m. Explored for oil shale (with MVT-style lead and zinc as secondary targets) on BARTON and OOLDEA.||||Disconformably overlies Loongana Formation.|6 m of inter-tidal grey sandy silts (carbonaceous top 0.5 m) with some shale interclasts, greenish grey shale bands lower in section gradually becoming sandier and ferruginous towards base; grey to black, in part carbonaceous, mudstone and shale.|
10987|Madura Formation|70397|5|Briefly described|p3|Cretaceous|Cretaceous|Bight Basin.||||Unconformably overlain by Hampton Sandstone. Underlain by Loongana Sandstone.||29-JUL-19
10987|Madura Formation|70771|5|Briefly described|p2, p27|Cretaceous|Cretaceous|Eucla Basin.||||Conformably overlies the Loongana Formation. Unconformably overlain by the Hampton Sandstone.|Siliciclastic sedimentary rocks.|
10987|Madura Formation|70772|4|Described|p2, p4-p9, p12-17|Albian|Valanginian|Madura Shelf. The most laterally extensive and thickest unit of the onshore Bight Basin. Achieves a maximum thickness of at least 355m in Madura 1, thickness is measured at 256m in SDDH001; two wells, Eucla 1 and BN1 preserve anomalously thing sections. In NDDH002 and Eucla 1 it disconformably overlies crystalline basement. Thins in the west and east of the basin but remains thick in centre of the basin. Bioclasts are common in some places. Age is derived from palnological data from parts of the base and top of the formation. Deposited primarily in  a lacustrinel non-marine environment with some evidence of later marine influence. Charcoal, fossil brachiopods, cephalopds, shell fragments and dinocysts are present. See also  p22-26, p28, p31, p33-34, p36, p38, p40-41.||||Conformably overlies the Loongana Formation, disconformably overlies the Shanes Dam Conglomerate. Unconformably overlain by the Hampton Sandstone and the Eucla Group.|Fine sandy micaceous base with occasional charcoal rich horizons that grade into glauconitic medium to coarse sand. Overlying this is homogenous light grey siltstone and minor beds of fine sands.|
10987|Madura Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, greensand|
10987|Madura Formation|71361|5|Briefly described|p5|Cretaceous|Cretaceous|Eucla Basin. Deposited in a marine environment when much of the Australian landmass was beneath the Eromanga Sea.||||Overlies the Loongana Sandstone. Unconformably overlain by the Hampton Sandstone.|Marine sandstones.|
10987|Madura Formation|71618|4|Described|p124-125,127-135,137|Albian|Early Cretaceous|Geological province: Bight Basin and Madura Shelf. Deposited during continued thermal subsidence and the most extensive unit in the Bight Basin. Depositional environment: non-marine, freshwater-brackish to intermittent marine. Thickness: at least 355m in Madura-1. Thickest in central basinal areas and generally thins toward basin margins. See p128 for isopachs. Samples from basal portions of the Madura Formation in both the HDDH001 (397.6-397.7 m) and FOR011 (256.8-257 m) yielded extremely similar assemblages to the Loongana Formation (Early Cretaceous) despite a separation of ~275 km. Uppermost sections in FOR011 (104.25-104.4 m) contained an extremely distinctive and rich dinocyst-dominated Albian palynomorph assemblage (Barham et al., 2016). U-Pb ICPMS zircon analysis yield major concordant age peaks at c. 1150 and 1650 Ma, similar to the Loongana Formation and Decoration Sandstone. Upper Madura Formation also yields a single concordant grain at c. 106 Ma, volcanic in origin and likely from an eruptive cloud from violent explosive eruptions around the Whitsundays.||||Disconformably overlain by Hampton Sandstone. Conformably underlain by Loongana Formation or disconformably underlain by Shanes Dam Conglomerate or crystalline basement.|Silts and fine sands, becoming increasingly glauconitic and bioturbated and fossiliferous at the top.|06-SEP-19
10987|Madura Formation|71891|5|Briefly described|p6-p7, p14, p29-p43, p45-p52, p54-p55|Late Cretaceous|Early Cretaceous|Bight basin, Coompana Province. 30-474m thick. Interpreted to have been deposited in a marine environment with limited circulation.||||Conformably overlies the Loongana Formation. Overlain by the Hampton Sandstone or Pidinga Formation unconformably.|Carbonaceous or glauconitic sandstone, siltstone, claystone and shale.|
10987|Madura Formation|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Barremian|Bight Basin.  Age from biostratigraphy.|||||Carbonaceous sandstone, siltstone, claystone and shale; commonly pyritic.|
10987|Madura Formation|72344|5|Briefly described|p4, p9, p13, p16, p49, p61|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474m. Interpreted to have been deposited in a marine environment with limited circulation. Intersected in drillhole CDP008. Petrography, SHRIMP analyses and geochemistry are discussed for a sample. Maximum depositional age is derived from SHRIMP dating in this volume. See also p84, p96, p107-p108, p110, p114, p169.|1147 +/- 5 Ma (Max dep. Age)|||Conformably overlies the Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone and claystone and shale; commonly pyritic.|04-SEP-19
10987|Madura Formation|72465|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Marine, low-energy lacustrine conditions.||||Conformably overlies Loongana Formation, or unconformably the Toolgana Supersuite.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72466|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Deposited in a marine, low-energy lacustrine environment.||||Conformably overlies Loongana Formation. Is overlain by Pidinga Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72467|5|Briefly described|p8, 17|Early Cretaceous|Early Cretaceous|Hill (1995). Bight Basin, Coompana Province. Up to 474m thick. Deposited in a marine, low-energy lacustrine environment.||||Conformably overlies Loongana Formation. Is overlain by Pidinga Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72468|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72469|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72470|5|Briefly described|p8, p18|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72471|5|Briefly described|p8, p17|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic.|
10987|Madura Formation|72472|4|Described|p8, p16-20|Early Cretaceous|Early Cretaceous|Bight Basin. Maximum thickness of 474 m. Deposited in a marine environment with limited circulation suggested by low-energy lacustrine conditions although observations from drillhole CDP008 indicate a non-marine setting. Interfingering transition with underlying Loongana Formation.||||Conformably underlain by Loongana Formation.|Carbonaceous or glauconitic sandstone, siltstone, and claystone and shale; commonly pyritic. Includes rip-up clasts of brown siltstone, irregular horizons of charcoal fragments, and red-brown medium to coarse grained sandstones and pebbly gravels.|
10987|Madura Formation|72947|6|Mentioned|p11|Cretaceous|Cretaceous|||||Overlies Koomalboogurra Suite.||
10987|Madura Formation|73084|5|Briefly described|p7, p16-19|Early Cretaceous|Early Cretaceous|Bight Basin. Typically between 150-200 m thick.||||Underlain by Loongana Formation and Shanes Dam Conglomerate. Unconformably[?] overlain by Hampton Sandstone.|Dark carbonaceous shale, siltstone and poorly consolidated minor sandstone.|
10987|Madura Formation|73232|6|Mentioned|p18|Early Cretaceous|Early Cretaceous|[May be] preserved in Eucla Basin palaeovalleys (Hou et al., 2008).||||||
10987|Madura Formation|73641|5|Briefly described|p4, 8-15, 17|Early Cretaceous|Early Cretaceous|Bight Basin. ~200m thick. Low-energy, limited circulation marine sedimentation. Mineralogical, element, TOC compositions tabulated.||||Overlies and interfingers with Loongana Formation.|Sandstones, carbonaceous sandstones, glauconitic sandstones, siltstones, and argillites, commonly pyritic.|
11034|Mainoru Formation|22538|6|Mentioned|Fig3 P708|||||||||
11034|Mainoru Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11034|Mainoru Formation|22853|3|Fully described|26|Proterozoic|Proterozoic|Of the Roper Group. Max thickness 200 m. Overlying unit Crawford Formation, underlying unit Limmen Sandstone||||||31-OCT-06
11034|Mainoru Formation|23216|5|Briefly described|Table1p8,34|||||||||
11034|Mainoru Formation|23374|5|Briefly described|p6||Calymmian|U/Pb Zircon age of 1494Ma. Of the Roper Group. In the McArthur Basin.||||||31-OCT-06
11034|Mainoru Formation|23404|5|Briefly described|p638|Calymmian|Calymmian|Age: 1492+/-4Ma.||||||31-OCT-06
11034|Mainoru Formation|23407|5|Briefly described|p633|||||||||
11034|Mainoru Formation|23733|5|Briefly described|p45 App.2|Mesoproterozoic|Mesoproterozoic|Of Roper Group.  Age: 1492+/-2Ma.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|23776|5|Briefly described|p711|||Of Roper Group.||||||
11034|Mainoru Formation|23937|2|Defined|p84 App. 1, p30-36, p23-24, p27,26, p6|Calymmian|Calymmian|Of the Roper Group.  Conformably overlain by Crawford Formation.  Age: 1492+/-4 Ma; 1493+/-4Ma (Jackson et al, 1999).  Max. thickness: <100m.  Geological Province: McArthur Basin.  See also p30.||||||10-NOV-17
11034|Mainoru Formation|24047|6|Mentioned|p23|||Contains the Wadjeli Sandstone Member.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
11034|Mainoru Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Siltstone: micaceous in places; interbedded with sandstone: fine-grained, thin to medium-bedded, glauconitic or pyritic in places, mudstone intraclasts; mudstone: carbonaceous, thin to very thin-bedded. Geol. Prov: McArthur Basin.||||||13-OCT-05
11034|Mainoru Formation|24050|3|Fully described|p42, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Calcareous and non-calcareous mudstone; glauconitic and micaceous siltstone and sandstone; limestone.  Overlies Limmen Sandstone; underlies Crawford Formation.  Thickness: ~250m.||||||31-OCT-06
11034|Mainoru Formation|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|24303|5|Briefly described|p59 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Age: 1492 +/- 4 Ma. Possible correlative of Grayling Member (Baralandji Formation) - see p61 Appendix.||||||
11034|Mainoru Formation|32660|5|Briefly described|Table 4|||||||||
11034|Mainoru Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11034|Mainoru Formation|40691|6|Mentioned|p65|||Mention Fig.4||||||
11034|Mainoru Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11034|Mainoru Formation|41220|6|Mentioned|Fig.3|||||||||
11034|Mainoru Formation|41268|6|Mentioned|p290|||||||||
11034|Mainoru Formation|41531|6|Mentioned|p167|||||||||
11034|Mainoru Formation|42385|4|Described|p26|||See also Table 5 p25.||||||31-OCT-06
11034|Mainoru Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
11034|Mainoru Formation|42597|5|Briefly described|Map Legend|Adelaidean||||||||
11034|Mainoru Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Lower Roper Group (Roper Group).||In schematic section, underlies Crawford Formation; overlies Limmen Sandstone.|Micaceous siltstone to sandstone, dolomitic siltstone, mudstone, micaceous siltstone to muddy siltstone, sandstone and siltstone. Detailed lithology given.|11-NOV-11
11034|Mainoru Formation|42639|4|Described|p38|||||||||
11034|Mainoru Formation|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
11034|Mainoru Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Interbedded red-brown to purple mudstone and very fine to fine grained sandstone both commonly micaceous and glauconitic.||||||19-OCT-05
11034|Mainoru Formation|42812|3|Fully described|p47, Table 5|||Of the Roper Group.||||||31-OCT-06
11034|Mainoru Formation|42846|5|Briefly described|p503, Fig.1 p502|||Oof Roper Group. Fine-grained. Geological Province: McArthur Basin.||||||09-MAY-05
11034|Mainoru Formation|43010|5|Briefly described|p164|||||||||
11034|Mainoru Formation|43036|4|Described|p59|||Of Roper Group.||||||31-OCT-06
11034|Mainoru Formation|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||31-OCT-06
11034|Mainoru Formation|43652|6|Mentioned|p386|||||||||
11034|Mainoru Formation|44112|3|Fully described|Table12p68,69-70|||||||||
11034|Mainoru Formation|44287|14|Not recorded|p.12, opp.11|||Glauconitic. (E53-3).||||||
11034|Mainoru Formation|44288|14|Not recorded|map legend|||Siltstone, glauconitic sandstone, feldspathic sandstone, shale. Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
11034|Mainoru Formation|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic, pt of Roper Gp.||||||
11034|Mainoru Formation|44332|14|Not recorded|p.7,opp.6,map|||(D53-14).||||||
11034|Mainoru Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
11034|Mainoru Formation|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Mt.Marumba Sheet. (D53-6).||||||
11034|Mainoru Formation|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44434|14|Not recorded|p.7, opp. p.6, map|||Includes Wooden Duck Member. (D53-11,12).||||||
11034|Mainoru Formation|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44436|5|Briefly described|p.11, opp. p. 7, map|||(E53-4).||||||02-DEC-04
11034|Mainoru Formation|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Laminated micaceous siltstone and fine-grained sandstone.  Conformably overlies Limmen Sandstone; conformably overlain by Crawford Formation.  Upper (?) Proterozoic.||||||08-DEC-04
11034|Mainoru Formation|44459|14|Not recorded|P.8,opp.p.6, map|||(E53-2).||||||
11034|Mainoru Formation|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44471|14|Not recorded|p.9,11,15,opp.7, map|||(D53-10).||||||
11034|Mainoru Formation|44472|5|Briefly described|map legend|||Of the Roper Group.  Micaceous siltstone, blocky chert, pink to cream silicified siltstone.  Upper (?) Proterozoic.||||||02-DEC-04
11034|Mainoru Formation|44473|14|Not recorded|p.10, opp. p.7|||(E53-7). Formation of Roper Group.||||||
11034|Mainoru Formation|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|44530|14|Not recorded|p.11, opp.12|||(D53-15).||||||
11034|Mainoru Formation|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
11034|Mainoru Formation|45022|6|Mentioned|p.80||Adelaidean|Of Roper Group.  Tb.11.||||||
11034|Mainoru Formation|45162|6|Mentioned|Fig.4|||||||||
11034|Mainoru Formation|46861|6|Mentioned|Fig.2|||||||||
11034|Mainoru Formation|46968|6|Mentioned|p304|||||||||
11034|Mainoru Formation|60483|5|Briefly described|p7 Fig. 5, p9|||Of the Roper Group. Age: 1492+/-4ma SHRIMP, Jackson et al 1999). Geological Province: McArthur Basin. Carbonaceous unit.||||||
11034|Mainoru Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Crawford Formation, underlain by Limmen Sandstone.||||||
11034|Mainoru Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Contains the Showell, Wooden Duck, Mountain Valley Limestone, Nullawun, Wadjeli Sandstone and Gibb Members.  Overlies Limmen Sandstone; underlies Crawford Fm.  Actual Mainoru Formation rocks are undifferentiated on this sheet area.||||||15-FEB-05
11034|Mainoru Formation|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlies the Limmen Sandstone. Overlain by the Crawford Formation. Green to grey micaceous siltstone, shale and fine-grained glauconitic sandstone.||||||
11034|Mainoru Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup.||||||
11034|Mainoru Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Siltstone: micaceous in places; interbedded with sandstone: fine-grained, thin to medium-bedded, glauconitic or pyritic in places, mud stone intraclasts; mudstone: carbonaceous, thin to very thin-bedded. Geol. Prov: McArthur Basin.||||||
11034|Mainoru Formation|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Mica-rich siltstone. Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|61572|5|Briefly described|p666|Mesoproterozoic|Mesoproterozoic|Of the lower Roper Group. Age: 1493Ma.  Geological Province: McArthur Basin.||||||
11034|Mainoru Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
11034|Mainoru Formation|63866|4|Described|p113, p116|Calymmian|Calymmian|McArthur basin.|1493 +/- 4 Ma (Jackson et al., 1999)|Roper Group|||Tuffite.|
11034|Mainoru Formation|64784|5|Briefly described|p2 Fig.2 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.||
11034|Mainoru Formation|64815|6|Mentioned|p5 Fig.3 |||||Of the Roper Group.||||
11034|Mainoru Formation|64816|5|Briefly described|p2 Fig.1,p4  |Calymmian|cCalymmian||1492 +/- 4 Ma.|Unit in Roper Group.||||
11034|Mainoru Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
11034|Mainoru Formation|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.|Includes Wooden Duck Member.|||
11034|Mainoru Formation|65228|5|Briefly described|Fig.02.|||||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.||
11034|Mainoru Formation|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
11034|Mainoru Formation|65337|6|Mentioned|p7, p45.|||McArthur Basin. Storm shelf facies closely resembles that of Crow Formation.|1492 +/- 4 Ma (Jackson et al. 1999).|||||
11034|Mainoru Formation|65340|4|Described|p11, p62.|Mesoproterozoic|Mesoproterozoic|A thick recessive unit, rarely well-exposed. The cross-bedded lithofacies is identical to Crawford Formation and was partially mis-mapped by Yates (1963). Reflects a mainly subtidal, storm-wave-influenced marine shelf environment.|1492 +/- 4 Ma (Jackson et al. 1999).|Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Interbedded green to grey micaceous mudstone and tabular lithic, glauconitic fine sandstone with basal markings; also resistant intervals of grey, pseudokarstically weathering, thick bedded lithic fine sandstone with swaley crossbeds.|
11034|Mainoru Formation|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 190 m.  Seen as having potential as an insulating layer for geothermal energy.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Siltstone, shale, fine sandstone.|
11034|Mainoru Formation|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Recessive.||Unit in Roper Group.||Overlies Limmen Sandstone. Is overlain by Crawford Formation.|Red-brown micaceous siltstone to very fine-grained sandstone; minor thin beds of dolomitic siltstone and light purple mudstone; minor glauconitic fine-grained sandstone and siltstone.|
11034|Mainoru Formation|67323|5|Briefly described|Mount Isa Block Time-Space Plot, p9|Mesoproterozoic|Mesoproterozoic|See also Eastern Australia Time-Space Plot. McArthur region (NT) and Camooweal-Murphy Domain, Mount Isa Inlier (QLD). Ages: 1492+/-4 Ma, 1493+/-4 Ma (Jackson et al. 1999).||||Correlated with South Nicholson Group||
11034|Mainoru Formation|67352|4|Described|p13, p47, p49|Calymmian|Calymmian|McArthur Basin. Over 1km thick.||Roper Group||Overlies Limmen Sandstone (conformably).  Overlain by Crawford Formation (conformably) or Buckalara Sandstone or Top Springs Limestone.|Siliceous siltstone and shale; micaceous siltstone and very finegrained sandstone: tabular to fissile and glauconitic; minor glauconitic fine-grained sandstone and siltstone.|
11034|Mainoru Formation|68146|6|Mentioned|p197|||Ages of tuffaceous layers; Jackson et al. (1999).|1492 +/- 4 Ma and 1493 +/- 4 Ma.|||||
11034|Mainoru Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian||1492 +/- 4 Ma.|Of Roper Group.||||
11034|Mainoru Formation|69430|4|Described|p15:3, 26-27, 30, 34, 48, 62|Calymmian|Calymmian|McArthur Basin. Abbott et al. (2001) divided the Formation into six named Members based on lithology. SHRIMP U-Pb zircon age for a tuffaceous bed.|1492 +/- 4 Ma (Jackson et al., 1999).|Collara Subgroup.|Gibb, Wadjeli Sandstone, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell, Members.|Conformably overlies Limmen Sandstone. Is ovelain conformably by Crawford Formation or disconformably by Jalboi Formation.|Red and green mudstone and siltstone, glauconitic and micaceous sandstone, micritic and intraclastic limestone, calcareous and non-calcareous mudstone.|12-JUL-16
11034|Mainoru Formation|69458|5|Briefly described|p42:21|||McArthur Basin.||Roper Group.||Is overlain unconformably by Annie Creek Limestone.||12-JUL-16
11034|Mainoru Formation|69591|5|Briefly described|p52||||1493 and 1492 +/- 4 Ma (Jackson et al., 1999).|||Corelated with the South Nicholson Group in Qld.||
11034|Mainoru Formation|69673|5|Briefly described|p16 fig 13, p31|||McArthur Basin. Unexplored source rock potential.|1492 +/- 4 Ma (SHRIMP)|Collara Subgroup||Overlain by Crawford Formation, Jalboi Formation, Overlies Limmen Sandstone|Tuffaceous bed.|
11034|Mainoru Formation|70734|5|Briefly described|p14, 16|||McArthur Basin.||Of Collara Subgroup.|Includes Gibb Member, Nullawun Member, Mountain Valley Limestone Member, Wooden Duck Member, Showell Creek Member.|||
11034|Mainoru Formation|70822|5|Briefly described|p102 fig 1 (A), p104|Mesoproterozoic|Mesoproterozoic|SHRIMP U-Pb zircon age from tuffs in Showell Mmeber.|1492 +/- 4 Ma (Southgate et al., 2000).|Roper Group.|Gibb, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell Creek, Members.|Overlies Limmen Sandstone; overlain by Crawford Formation.||24-SEP-18
11034|Mainoru Formation|70897|5|Briefly described|p44, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|This age, and another at 1493 +/- 4 Ma, represent a maximum depositional age and effectively the actual deposition age.|1492 +/- 4 Ma.|Roper Group.|||Includes green claystone (?tuffs) from dark grey, laminated, low-energy (deep-water) shales.|
11034|Mainoru Formation|70968|2|Defined|p6, p13, p17-35, p44, p53, p69, p123|Calymmian|Calymmian|See also p126, p130-131, p143. Sweet in Abbott et al. (2001) after Dunn (1963). Named after Mainoru homestead. Originally mapped as middle part of Wigram Formation of Malay Road Group (Dunnet, 1965) and as upper part of Baralminar beds (Plumb and Roberts, 1992): these names are now superseded. Partially mismapped as Crawford Formation by Yates (1963) in ROBINSON RIVER sheet. Type section is SE of Mountain Valley homestead at 372100mE 8444000mN (base) through 373600mE 8437600mN then SE to 379600mE 8433200mN (top), in URAPUNGA sheet. The usefulness or otherwise of subdividing the Formation is discussed. Very recessive: forms rubble- and scree-covered valleys. Widely distributed. Variable thickness up to c.1000m. Fluvial floodplain to shallow-marine facies. Is intruded by Derim Derim Dolerite sills.|1492 +/- 4 Ma (Jackson et al., 1999).|Collara Subgroup.|Wadjeli Sandstone, Wooden Duck, Mountain Valley Limestone, Nullawun, Gibb, Showell, Members.|Overlies Limmen Sandstone and Mantungula Formation conformably (locally disconformably). Underlies Crawford Formation gradationally, and Buckingham Bay Sandstone or Jalboi Formation unconformably.|A complex unit dominated by red, green, grey and black shale and siltstone, with lesser glauconitic and micaceous sandstone, micritic and intraclastic limestone, and calcareous mudstone. Carbonates are minor and atypical of Roper Group.|
11034|Mainoru Formation|71059|4|Described|p3, p14-16, p18, p20, p24, p31|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 270-1000m thick. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, organic petrology reflectivity, data all detailed.||Collara Subgroup.|Gibb, Wadjeli Sandstone, Nullawun, Mountain Valley Limestone, Wooden Duck, Showell, Members.|Conformably overlies Limmen Sandstone. Is overlain conformably by Crawford Formation, and unconformably to disconformably by Jalboi Formation.|Non-calcareous and calcareous mudrocks, glauconitic and micaceous sandstone, micritic and intraclastic limestone.|
11034|Mainoru Formation|71369|6|Mentioned|p4|||Ages are U-Pb and interpreted as depositional ages for the tuffs of this formation.|1492 +/- 4 Ma and 1493 +/- 4 Ma|||||
11034|Mainoru Formation|71488|5|Briefly described|p141 fig 1b, p142|Calymmian|Calymmian|Dated at 1492 +/- 4 Ma and 1492 +/- 29 Ma by Jackson et al., 1999 and Southgate et al., 2000, respectively.|c. 1492 Ma (SHRIMP)|Collara Subgroup|Includes the Gibb Member, Nullawan Member, Mountain Valley Limestone Member, Wooden Duck Member and the Showell Creek Member.|Overlies the Limmen Sandstone. Overlain by the Crawford Formation.||
11034|Mainoru Formation|71494|4|Described|p2-p27|||Intersected by six HyLogged holes. Crops out in an ENE-trending belt in northwestern Urapunga. Originally defined by Abbott et al (2001) who also defined new members. Core log features presented in this volume.|||Includes the Mountain Valley Limestone Member, Wooden Duck Member, Nullawun Member and the Showell Member.||Comprises red, green grey and black shale and siltstone, glauconititc and micaceous sandstone, micritic and intraclastic limestone and calcareous mudstone.|
11034|Mainoru Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1492+/-4 Ma (crystallisation: U-Pb zircon).||||Tuffite, tuff.|
11034|Mainoru Formation|71779|5|Briefly described|p2, p23, p24, p26, 27|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin. SHRIMP U-Pb zircon age from tuffs in Showell Member.|1492 +/- 4 Ma, 1493+/-4 Ma (Jackson et al., 1999)|Collara Subgroup|Includes the Showell Member, Wooden Duck Member, Mountain Valley Limestone Member, Nullawun Member, Wadjeli Sandstone Member, Kilgour Sandstone Member, and Gibb Member.|||24-SEP-18
11034|Mainoru Formation|71893|4|Described|p5, p8-p9, p13, p17, p20, p25, p32|Calymmian|Calymmian|McArthur Basin.||Collara Subgroup|Includes the Showell Member.|Conformably (locally disconformably) overlies the Limmen Sandstone. Conformably overlain by the Crawford Formation.||
11034|Mainoru Formation|72526|5|Briefly described|p3, p8 Fig.1.3, p85,|Calymmian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Includes tuffs dated at 1492 +/- 4 Ma and 1493 +/- 4 Ma.|1493 +/-4 Ma to 1492 +/-4 Ma|Collara Subgroup||Overlies Limmen Sandstone and underlies Crawford Formation.||
11034|Mainoru Formation|72527|5|Briefly described|p1, p10, p41, p56, p65.|Calymmian|Calymmian|Tuffs dated at 1492 +/- 4 Ma and 1493+/- 4 Ma (Jackson et al. 1999).|younger than c. 1492 Ma|Collara Subgroup|||Includes tuffs.|
11034|Mainoru Formation|72718|6|Mentioned|p7, p9|Calymmian|Calymmian|Southern McArthur Basin.|1492 +/- 4 Ma|Collara Subgroup, Roper Group|Showell Member|Partly underlain by Limmen Sandstone. Overlain by Crawford Formation.||
11034|Mainoru Formation|72912|5|Briefly described|p5 Fig.3, p20.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Age determined using volcanic tuff samples; ref Jackson et al., 1999. U-Pb zircon sedimentary depositional age (Ma).|1492 +/- 4 Ma, 1493 +/- 4 Ma|Collara Subgroup||Overlies Limmen Sandstone and underlies Crawford Formation.|Includes tuffs.|
11034|Mainoru Formation|73042|6|Mentioned|p4|Calymmian|Calymmian|Southern McArthur Basin, Roper Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1492+/-4 Ma and 1493+/-4 Ma|Collara Subgroup, Roper Group||Underlain by Limmen Sandstone. Overlain by Crawford Formation.||
11034|Mainoru Formation|73083|6|Mentioned|p47|Mesoproterozoic|Mesoproterozoic|||||||
11034|Mainoru Formation|73242|5|Briefly described|p39|Calymmian|Calymmian||ca 1492 Ma|Collara Subgroup, Roper Group|Showell Member, Wooden Duck Member, Moutain Valley Limestone Memebr, Nullawun Member, Wadjeli Sandstone Member, Gibb Member|Underlain by Limmen Sandstone. Overlain by Crawford Formation. Intruded by Derim Derim Dolerite.|Includes felsic volcanic rocks, interbedded mudstone and fine sandstone, marine shelf sandstone, mudstone and shale, and limestone in mudstone.|
11034|Mainoru Formation|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].||||||
11034|Mainoru Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Collara Subgroup.||Overlies Limmen Sandstone and Mantungula Formation. Is overlain by Crawford Formation.||
11092|Malgabbie Formation|41594|4|Described|p68|||||||||
11115|Mallens Sandstone|14228|6|Mentioned|p8|Kungurian|Kungurian|||Byro Group||||
11115|Mallens Sandstone|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
11115|Mallens Sandstone|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
11115|Mallens Sandstone|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
11115|Mallens Sandstone|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
11115|Mallens Sandstone|23726|5|Briefly described|p49 Fig 15|Early Permian|Early Permian|Of Byro Group. Overlying unit Bulgadoo Shale. Underlying unit Coyrie Formation. Geological Province: Carnarvon Basin.||||||
11115|Mallens Sandstone|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
11115|Mallens Sandstone|37000|6|Mentioned|p23|||||||||
11115|Mallens Sandstone|37294|6|Mentioned|p100|||||||||
11115|Mallens Sandstone|37295|6|Mentioned|p51|||Proposed usage.||||||
11115|Mallens Sandstone|37304|6|Mentioned|p55|||||||||
11115|Mallens Sandstone|38493|6|Mentioned|p36|||||||||
11115|Mallens Sandstone|39316|6|Mentioned|Fig.2|||||||||
11115|Mallens Sandstone|40617|6|Mentioned|Fig.1|||||||||
11115|Mallens Sandstone|41271|3|Fully described|p95|||||||||
11115|Mallens Sandstone|41438|6|Mentioned|Fig.11|||||||||
11115|Mallens Sandstone|42116|5|Briefly described|p38|||||||||
11115|Mallens Sandstone|42392|6|Mentioned|p119|||See also Mallens Formation P116 Byro Group||||||
11115|Mallens Sandstone|42734|5|Briefly described|map legend|Permian||||||||
11115|Mallens Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
11115|Mallens Sandstone|43255|5|Briefly described|map legend||Artinskian|of Byro Group.||||||
11115|Mallens Sandstone|43256|5|Briefly described|5-22||Permian|||||||
11115|Mallens Sandstone|45168|6|Mentioned|p6|||||||||
11115|Mallens Sandstone|49644|5|Briefly described|Table|||||||||
11115|Mallens Sandstone|60331|5|Briefly described|p33 Fig.2|Kungurian|Artinskian|Of Byro Group. Overlies Coyrie Formation. Overlain by Bulgadoo Shale. Geological Province: Southern Carnarvon Basin.||||||
11115|Mallens Sandstone|64580|5|Briefly described|map legend|||Of Lower Byro Group. Fine-grained biturbated sandstone overlying interbedded sandstone, siltstone and mudstone.||||||15-DEC-08
11115|Mallens Sandstone|64974|6|Mentioned|p147 Fig. 5|Kungurian|Artinskian|Geological Province: Carnarvon Basin.||||||24-JUN-09
11115|Mallens Sandstone|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.||Unit in Byro Group.||Overlies Coyrie Formation.|Fine- to medium-grained sandstone; minor siltstone; characteristically intensely bioturbated.|
11115|Mallens Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey/light grey sandstone, finely laminated, pin stripe laminations 25%; dark brown siltstone/sandstone heavily bioturbated 75%.|
11115|Mallens Sandstone|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 2.69 W/mK. See also p47, p54, app 2 p6.||Byro Group||Overlies Coyrie Formation, overlain by Bulgadoo Shale|Bioturbated sandstone with hummocky stratification.|
11115|Mallens Sandstone|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.||Overlain by the Bulgadoo Shale. Underlain by the Coyrie Formation.|Comprises fine- to medium-grained sandstone; minor siltstone; characteristically intensely bioturbated.|
11115|Mallens Sandstone|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Coyrie Formation as one unit.||Of the Byro Group.|||Fine-grained bioturbated sandstone overlying interbedded sandstone, siltstone and mudstone.|15-AUG-18
11115|Mallens Sandstone|69166|4|Described|geologyp_lut.csv|Kungurian|Kungurian|||Byro Group|||Fine- to medium-grained sandstone; minor siltstone; characteristically intensely bioturbated|
11115|Mallens Sandstone|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Coyrie Formation.||Byro Group.|||Fine-grained bioturbated sandstone overlain by interbedded sandstone, siltstone and mudstone.|
11115|Mallens Sandstone|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group|||Fine- to medium-grained sandstone; minor siltstone; characteristically intensely bioturbated.|
11115|Mallens Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, greywacke|
11115|Mallens Sandstone|72910|4|Described|p18, p23, p33, p39, p41.|Kungurian|Kungurian|Thickness 60-200m. Type section located in Northern Kennedy Range, 24d05mS; 115d07mE. Said to be Artinskian age p39.||Byro Group.||Conformably overlies Coyrie Formation. Conformably underlies Bulgadoo Shale.|Fine to medium sandstone, minor siltstone, commonly intensely bioturbated.|
11129|Malouet Formation|13615|6|Mentioned|p82|||||||||
11129|Malouet Formation|23379|4|Described|p160 Fig.2;p158,159,162,163,165,167-174||Berriasian|of Barrow Group, Barrow Sub-basin, Carnarvon Basin.||||||
11129|Malouet Formation|23726|5|Briefly described|p8 Fig 2c|Early Cretaceous|Early Cretaceous|Overlying unit Flacourt Formation. Geological Province: Carnarvon Basin.||||||
11129|Malouet Formation|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Early Cretaceous|Overlies Dupuy Formaiton. Conformably overlain by Flacourt Formation. Marine. Geological Province: Barrow Sub-basin.||||||
11129|Malouet Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
11129|Malouet Formation|37685|6|Mentioned|p6|||||||||
11129|Malouet Formation|40617|6|Mentioned|p11|||||||||
11129|Malouet Formation|41271|3|Fully described|p138|||||||||
11129|Malouet Formation|41438|6|Mentioned|p108|||||||||
11129|Malouet Formation|41440|4|Described|p137|||||||||
11129|Malouet Formation|41445|5|Briefly described|p192|||||||||
11129|Malouet Formation|41447|6|Mentioned|p227|||||||||
11129|Malouet Formation|41732|6|Mentioned|p540|||||||||
11129|Malouet Formation|41751|6|Mentioned|p5|||||||||
11129|Malouet Formation|42116|5|Briefly described|Fig.1 P6|||||||||
11129|Malouet Formation|42598|3|Fully described|p91|||Age early to latest Berriasian||||||
11129|Malouet Formation|42615|5|Briefly described|p37|||lower Barrow Group.||||||
11129|Malouet Formation|43712|5|Briefly described|p11|||||||||
11129|Malouet Formation|43722|5|Briefly described|p10|||||||||
11129|Malouet Formation|43724|5|Briefly described|p29|||||||||
11129|Malouet Formation|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin (Dampier Sub-basin).||||||
11129|Malouet Formation|64977|6|Mentioned|p493 Fig.3.|Early Cretaceous|Early Cretaceous|Thevenard Island area.||||||
11129|Malouet Formation|67200|5|Briefly described|p8 fig 6, |Cretaceous|Cretaceous|||Barrow Group||Overlain by Flacourt Formation|Crudely and trough cross bedded, interbedded sandstone and siltstone.|
11129|Malouet Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Is overlain by Upper Barrow Group.||
11129|Malouet Formation|70066|5|Briefly described|Regional: p6|Early Cretaceous|Early Cretaceous|Barrow Sub-basin, Northern Carnarvon Basin. Oil reservoir.||Barrow Group.||||
11133|Malu Formation|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Lamil Group, Yeneena Basin||||||
11133|Malu Formation|23758|4|Described|p7|Neoproterozoic|Neoproterozoic|Of Lamil Group. Geological Province: Yeneena Basin.||||||
11133|Malu Formation|23780|5|Briefly described|p181|Mesoproterozoic|Mesoproterozoic|Of the Lamil Group.||||||
11133|Malu Formation|41066|5|Briefly described|1 of 2 A02|||||||||
11133|Malu Formation|42161|6|Mentioned|p49|||||||||
11133|Malu Formation|60470|5|Briefly described|p4, Fig. 2, p7, p9,  10-11, 14|Neoproterozoic|Neoproterozoic|in Yeneena Basin, base of Lamil Group. Conformably overlain by Puntapunta Formation. Sandstone; minor conglomerate, siltstone, and shale. ?Hosts Telfer gold mineralization.||||||
11133|Malu Formation|62453|3|Fully described|p5 Fig. 3, 68|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Lamil Group. Previously Malu Quartzite. Sandstone, siltstone, shale, dolomite. Conformably overlain by Puntapunta Formation. Thickness 2km. Conformably underlies Puntapunta Formation.||||||
11133|Malu Formation|62986|6|Mentioned|p18|||Geological Province: Yeneena Basin.||||||
11133|Malu Formation|64580|4|Described|map legend||Neoproterozoic|Of Lamil Group. Fine- to medium-grained quartz sandstone.||||||09-DEC-08
11133|Malu Formation|64725|5|Briefly described|p68.|Neoproterozoic|Neoproterozoic|Contains stratabound Au-Cu reef deposits, linked by stockwork of quartz-sulfide veins and sheeted vein sets. High-grade mineralisation due to supergene enrichment extends to 300 m below surface.||Unit in Lamil Group.|||Calcareous and carbonaceous siltstones interbedded with massive sandstone; stratabound Au-Cu bearing quartz-sulfide reefs.|
11133|Malu Formation|64777|4|Described|p3 Fig.4, p4-8|Neoproterozoic|Neoproterozoic|Turbiditic to deltaic. At least 1.5 km 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 Lamil Group|||Massive to well-bedded, fine- to coarse-grained sandstone interbedded with siltstone, shale and rare carbonate units.|
11133|Malu Formation|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin. Age: 920-915 Ma, maximum depositional age, SHRIMP U-Pb detrital zircon.|see comments|Lamil Group||Overlies Coolbro Sandstone (Throssell Range Group). Is overlain by Puntapunta Formation.||
11133|Malu Formation|65454|4|Described|p7-9, p11, p13, p19, p23, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of Lamil Group. Turbiditic sandstone interbedded with calcareous siltstones. Hosts the Telfer Cu-Au deposit in bedding-parallel quartz reefs. Includes Telfer Member.||||||
11133|Malu Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Lamil Group. Includes Telfer Member. Fine- to medium-granied quartz sandstone. Minor interbedded shale and dolomite. This unit, and its Telfer Member, are overlain by Puntapunta Formation.  Age <1070 Ma. Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
11133|Malu Formation|65826|5|Briefly described|p1, p13.|Neoproterozoic|Neoproterozoic|At least 2 km thick. Deep-water turbidite deposits in northeasterly prograding submarine fans. Fractured and sheared sandstones may contain significant groundwater supplies.||Unit in Lamil Group.|Includes Telfer Member.|Is overlain by Puntapunta Formation.||
11133|Malu Formation|67202|4|Described|p7, p59, p75, p117, p128, p156-157, p179|||See also p183, p189-192, p196, p198-199, p203, p208, p281. Yeneena Basin. 1-2 km thick. An aquifer supplying water to the Telfer mining community. Conductance image. Hosts Au-Cu deposits (esp. the Telfer Au-Cu mine). Appears as Marlu Formation on p7, and as Malu Quartzite on p190.||Basal Lamil Group.|Telfer Member.|Is overlain conformably by Puntapunta Formation.|Shale, sandstone and siltstone with thin carbonate units present towards the top.|
11133|Malu Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Yeneena Basin.||Lamil Group.||||
11133|Malu Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Lamil Group|||Fine- to medium-grained quartz sandstone.|
11133|Malu Formation|69590|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Events: Musgrave Orogeny; Paterson Orogeny.|1000-541 Ma (inferred)|Unit of Lamil Group.|Includes Telfer Member.||Fine- to medium-grained quartz sandstone|
11133|Malu Formation|71080|6|Mentioned|p26|||Yeneena Basin. Probable Tonian age.||Of Lamil Group.||||
11133|Malu Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
11133|Malu Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Neoproterozoic|Yeneena Basin.||Lamil Group.|||Fine- to medium-grained quartz sandstone.|
11165|Mandu Limestone|23726|5|Briefly described|p90|Miocene|Oligocene|Geological Province: Carnarvon Basin.||||||
11165|Mandu Limestone|24084|5|Briefly described|p146 Fig.2|Miocene|Miocene|Geological Province: North Carnarvon Basin.||||||16-MAR-05
11165|Mandu Limestone|40617|5|Briefly described|p14|||||||||
11165|Mandu Limestone|41271|3|Fully described|p176|||||||||
11165|Mandu Limestone|41437|6|Mentioned|p72|||||||||
11165|Mandu Limestone|41438|6|Mentioned|Fig.23|||||||||
11165|Mandu Limestone|41732|6|Mentioned|Fig.3|||||||||
11165|Mandu Limestone|42116|5|Briefly described|p70|||||||||
11165|Mandu Limestone|44959|4|Described|p.21||Miocene|||||||
11165|Mandu Limestone|48831|14|Not recorded|p.14,26,28,29|||||||||
11165|Mandu Limestone|61155|5|Briefly described|p15|Early Miocene|Early Oligocene|Of the Cape Range Group. Age: <33Ma. Max. thickness (offshore): 780m. Geological Province: Carnarvon Basin /onshore and offshore.||||||
11165|Mandu Limestone|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Overlies Robe Pisolite, Merlinleigh Sandstone, Giralia Calcarenite,|Crudely bedded limestone.|
11165|Mandu Limestone|68811|5|Briefly described|p108 fig 62, p191|Tertiary|Tertiary|Shown as Mandu Formation p107.||Base of Cape Range Group.||||16-APR-20
11165|Mandu Limestone|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Miocene|Oligocene|See also Regional: Fig.6. Northern Carnarvon Basin.||Cape Range Group.||Overlies Giralia Calcarenite and Walcott Formation. Is overlain by Trealla Limestone.||
11165|Mandu Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||marl, calcarenite|
11171|Manganese Group|24025|4|Described|p15|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Geological Province: Collier Basin.||||||22-MAY-08
11171|Manganese Group|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Parent: Bangemall Supergroup. Geological Province: Collier Basin||||||22-MAY-08
11171|Manganese Group|24183|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|Superseded by the Manganese Subgroup (Muhling and Brakel, 1985). Of the Bangemall Supergroup.||||||24-JUL-07
11171|Manganese Group|24535|6|Mentioned|p3 Fig. 1, p19 Fig. 15.|||Shown as part of the 'Mesoproterozoic basins', distinct from Edmund and Collier Basins.||||||26-NOV-13
11171|Manganese Group|30503|6|Mentioned|Fig.2|||||||||
11171|Manganese Group|30881|6|Mentioned|p527|||||||||
11171|Manganese Group|31393|6|Mentioned|Pl.25|||||||||
11171|Manganese Group|33536|6|Mentioned|p84|||||||||
11171|Manganese Group|33544|6|Mentioned|p30|||See also Plate 2. Middle Prot.||||||
11171|Manganese Group|34135|4|Described|Table 1|Mesoproterozoic|Mesoproterozoic|See also Table 2, pp6,7,13-18 etc. Middle Proterozoic.||||||24-JUL-07
11171|Manganese Group|35269|6|Mentioned|p304|||||||||
11171|Manganese Group|36884|4|Described|p156|||||||||
11171|Manganese Group|37460|3|Fully described|p122|||||||||
11171|Manganese Group|37577|6|Mentioned|p36|||||||||
11171|Manganese Group|37707|6|Mentioned|p13|||||||||
11171|Manganese Group|39697|6|Mentioned|p130|||||||||
11171|Manganese Group|40888|6|Mentioned|p154|||||||||
11171|Manganese Group|41669|3|Fully described|p34|||Also Mention on p10.||||||24-JUL-07
11171|Manganese Group|41768|6|Mentioned|p36|||||||||
11171|Manganese Group|42020|4|Described|p316|||||||||
11171|Manganese Group|42352|5|Briefly described|p28, p31|||||||||
11171|Manganese Group|43055|4|Described|p20, Table 4|||||||||
11171|Manganese Group|43056|5|Briefly described|Map Legend|||||||||
11171|Manganese Group|43595|6|Mentioned|p219||Paleoproterozoic|||||||07-NOV-08
11171|Manganese Group|44139|6|Mentioned|p277|||Northeasterly extension of Bangemall Group (Williams & Tyler 1989). Now Manganese Subgroup, Bangemall Group.|| ||||10-SEP-12
11171|Manganese Group|44297|14|Not recorded|p.5,6,7,10,12|||(F51-9). Equiv. of Waltha Woora Beds. (p.7). See also p. 18,19,20.||||||
11171|Manganese Group|44438|14|Not recorded|map legend||Mesoproterozoic|M.Proterozoic.||||||
11171|Manganese Group|50008|6|Mentioned|p44 Fig.1|||||||||
11171|Manganese Group|50010|5|Briefly described|p54|Mesoproterozoic|Mesoproterozoic|Correlates to Collier Group. Of Bangemall Supergroup.||||||
11171|Manganese Group|50188|6|Mentioned|p17|||Intruded by Davis Dolerite on BALFOUR DOWNS.||||||16-JUL-08
11171|Manganese Group|50225|5|Briefly described|p386 Fig. 1, p388|||Correlated with Bangemall Supergroup.  Geological Province: south-east Pilbara Craton.||||||07-FEB-11
11171|Manganese Group|60535|5|Briefly described|p556|Mesoproterozoic|Mesoproterozoic|Age: ca. 1070 Ma. Of the Bangemall Supergroup.||||||
11171|Manganese Group|62289|6|Mentioned|p4|||||||||
11171|Manganese Group|62453|6|Mentioned|p53|||Geological Province: Collier Basin.||||||
11171|Manganese Group|63139|5|Briefly described|p50|Mesoproterozoic|Mesoproterozoic|Overlies Pinjian Chert Breccia. Consists of fine-grained sedimentary rocks of shallow marine/lagoonal origin.||||||07-FEB-08
11171|Manganese Group|63417|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup.  Includes Woblegun Formation and undivided sedimentary unit which includes intrusions of Davis Dolerite. Geological Province: Collier Basin.||||||
11171|Manganese Group|64283|6|Mentioned|p50 Fig. 1, p53|||Hosts manganese and copper deposits.||||||07-FEB-11
11171|Manganese Group|64580|4|Described|map legend||Mesoproterozoic|Of Bangemall Supergroup. Sandstone, siltstone, mudstone, conglomerate, chert and dolostone.||||||09-DEC-08
11171|Manganese Group|64635|6|Mentioned|p2 Fig.1|||||||||
11171|Manganese Group|64772|6|Mentioned|p14 Fig. 7|||Shown only on map and not in legend.||||||07-FEB-11
11171|Manganese Group|64777|6|Mentioned|p1 Fig.2|Proterozoic|Proterozoic|||||||
11171|Manganese Group|65724|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Sedimentary rocks. Geol. Prov: Collier Basin.||||||
11171|Manganese Group|65829|4|Described|p1, p7 Fig.3, p10, p27, pp35-36.|Mesoproterozoic|Mesoproterozoic|Fluvial and marine sedimentary rocks. Small areas of unmetamorphosed sedimentary rocks in the Ripon Hills and Gregory Range Inlier, in the Collier Basin, are possible correlates. The Group unconformably borders the southeast part of the Pilbara Craton and the Northeast Pilbara Sub-basin of the Hamersley Basin. Onlaps the Pinjian Chert Breccia. In the Ripon Hills area, hosts manganese mineralization which overlies or replaces remnants of shale belonging to this Group; the ores have a high Fe content.|>1070 Ma.|Unit in Bangemall Supergroup.|Includes Coondoon and Woblegun Formation.|||
11171|Manganese Group|65830|6|Mentioned|p18|||Includes 'strings of beads' megafossils.|||Includes Stag Arrow Formation.|||
11171|Manganese Group|66107|5|Briefly described|p1,p4 Fig.1,p5, |Mesoproterozoic|Mesoproterozoic|No geochronological constraints on age but its relative stratigraphic position suggests that it is of similar age to the Collier Group.|||Includes the Balfour Formation, Jigalong Formation, Enachedong Dolomite, Stag Arrow Formation, Whitewood Formation and Woblegun Formation|Possible correlative of Collier Group.||
11171|Manganese Group|66427|6|Mentioned|p40 Fig.1|||Deposition 1.20->1.07 Ga.||||||
11171|Manganese Group|67202|5|Briefly described|p258|Mesoproterozoic|Mesoproterozoic|||Bangemall Supergroup.|Woblegun Formation.|||
11171|Manganese Group|67829|5|Briefly described|pp448-449, p453.|||Locally infills karst hollows in underlying Carawine Dolomite.||||Overlies Pinjian Chert Breccia.||
11171|Manganese Group|68902|6|Mentioned|p20|Mesoproterozoic|Mesoproterozoic|Intruded by dolerite sills at c.523-518 Ma.||||||
11171|Manganese Group|69003|5|Briefly described|p4, p53, p72|||Oakover Basin, Capricorn Orogen. Contemporaneous with Collier Group. Intruded by dolerites of the c.1070 Ma Warakurna LIP and contain economically significant Mn deposits.||||||
11171|Manganese Group|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|||Bangemall Supergroup|Includes Woblegun Formation||Interbedded, poorly sorted granule and pebble polymict conglomerate and coarse- to medium-grained lithic and quartz sandstone.|
11171|Manganese Group|69185|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Proterozoic|Of Collier Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 1070-1211 Ma|Unit of Bangemall Supergroup.|||Undivided; sandstone, siltstone, mudstone, conglomerate, chert and dolostone|
11171|Manganese Group|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Events: Western Australian events. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1465-1070 Ma (inferred)|Unit of Bangemall Supergroup.|Includes Woblegun Formation.||Fine- to coarse-grained lithic and quartz-rich sandstone; locally glauconitic; interbedded with micaceous siltstone; interbedded with granule and pebbly polymict conglomerate; mudstone and siltstone, shale; ferruginous, manganiferous.|
11171|Manganese Group|69596|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||||||
11171|Manganese Group|70826|6|Mentioned|p5 tbl 2, p10, p11|Mesoproterozoic|Mesoproterozoic|Collier Basin. Capricorn Orogen.||Bangemall Supergroup||||20-MAY-20
11171|Manganese Group|70936|5|Briefly described|p58-p59,61,72,74,77|Mesoproterozoic|Mesoproterozoic|Geological province: Pilbara Craton. Of Collier Basin. Correlable with Collier Group, and therefore probably deposited at, or shortly before c. 1070 Ma.|>1070 Ma|Unit of Bangemall Supergroup.|||Fine-grained sedimentary rocks.|16-AUG-19
11171|Manganese Group|71003|5|Briefly described|p58-p59, p61, p72, p74, p77|Mesoproterozoic|Mesoproterozoic|Pilbara Craton. Interpreted as part of the newly named Wongawobbin Basin.||Bangemall Supergroup|Includes the Stag Arrow Formation.|Partially correlated with the Collier Group.|Fine-grained sedimentary rocks.|
11171|Manganese Group|71042|4|Described|p63, p64 fig 1, p65-p67|Mesoproterozoic|Mesoproterozoic|Oakover Basin. See also Manganese Subgroup. Manganese deposits and deposit characteristics discussed in detail. See also p69-p77, p79-p91, p94-p98. Min age from K-Ar on glauconite in Coondoon Formation said to represent intrusion by Davis Dolerite. Max age from a tuffaceous unit near the base of the Manganese Group.|Max age: 1317 +/-11 Ma, min ~1050 Ma.||Includes the Coondoon Formation, Stag Arrow Formation, Balfour Formation, Enachedong Dolomite.|Unconformably overlies the Carawine Dolomite and the Pinjian Chert Breccia. Unconformably overlain by the Googenhama Formation.||24-MAY-19
11171|Manganese Group|71169|5|Briefly described|p71, p79-p80|Ectasian|Ectasian|East Pilbara, West Australian Craton. Deposited in shallow marine to marine siliciclastic settings.|c. 1300 Ma|||||
11171|Manganese Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, conglomerate, sandstone|
11171|Manganese Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Collier Basin.|max age 1317+/-11 Ma, min ~1070 Ma.|Bangemall Supergroup|Includes Woblegun Formation.||Sandstone, siltstone, mudstone, conglomerate, chert, and dolostone.|
11171|Manganese Group|72705|6|Mentioned|p3|||Capricorn Orogen.||||||
11241|Mararoa Pillow Lava Member|30562|4|Described|p40|||See also p37||||||09-AUG-05
11241|Mararoa Pillow Lava Member|43162|6|Mentioned|6|||||||||
11258|Marcenie Sandstone|36551|6|Mentioned|Table 13|||||||||
11264|Marda Complex|22481|6|Mentioned|p972|||||||||
11264|Marda Complex|23143|5|Briefly described|p191|||||||||
11264|Marda Complex|23159|6|Mentioned|p789|Archean|Archean|Maybe Informal||||||07-NOV-08
11264|Marda Complex|23441|6|Mentioned|p163|||||||||
11264|Marda Complex|23526|6|Mentioned|p4 Fig. 2|||||||||
11264|Marda Complex|23531|3|Fully described|p11-12|||SHRIMP U-Pb 2733 Ma.  Also see p15 + 21. Yilgarn Craton Province.||||||
11264|Marda Complex|23532|5|Briefly described|Map legend||Archean|Age: c.2733 Ma. Yilgarn Craton.||||||07-NOV-08
11264|Marda Complex|23780|5|Briefly described|p78|Archean|Archean|Age: ~2730+/-4 Ma||||||07-NOV-08
11264|Marda Complex|23787|4|Described|p9|Archean|Archean|Geological Province: Southern Cross Terrane.||||||07-NOV-08
11264|Marda Complex|24167|3|Fully described|p15, p7 Fig.3, p31 Fig.20|Archean|Archean|Age: c.2730 Ma (SHRIMP U-Pb zircon: Nelson, 2001 and Pidgeon and Wilde, 1990).  Intruded by Butcher Bird Monzogranite.||||||10-MAY-21
11264|Marda Complex|24245|5|Briefly described|p4, p7 Tb. 1|Archean|Archean|See also p16. Felsic volcanic rocks.  Age: c.2730Ma (SHRIMP U-Pb zircon, Pidgeon and Wilde, 199; Nelson, 2001).  Geological Province: Yilgarn Craton.||||||07-NOV-08
11264|Marda Complex|24335|5|Briefly described|Map legend|Archean|Archean|Age: >2733Ma.  Geological Province: Yilgarn Craton||||||07-NOV-08
11264|Marda Complex|24445|4|Described|p1|Archean|Archean|Age: 2.73Ga. Geological Province: Yilgarn Craton||||||07-NOV-08
11264|Marda Complex|24446|5|Briefly described|Map legend|Archean|Archean|Age: >2733Ma. Geological Province: Yilgarn Craton.||||||12-AUG-13
11264|Marda Complex|24530|6|Mentioned|p2 Fig. 1|||||||||
11264|Marda Complex|29784|6|Mentioned|p27|||||||||
11264|Marda Complex|30440|6|Mentioned|Table 6|||||||||
11264|Marda Complex|36007|6|Mentioned|p1128|||||||||
11264|Marda Complex|38012|6|Mentioned|p84|||||||||
11264|Marda Complex|38480|4|Described|p18|||||||||
11264|Marda Complex|38483|3|Fully described|p17|||||||||
11264|Marda Complex|39580|6|Mentioned|p308|||||||||
11264|Marda Complex|39869|6|Mentioned|p344|||||||||
11264|Marda Complex|40770|5|Briefly described|p418|||||||||
11264|Marda Complex|40930|6|Mentioned|p8|||||||||
11264|Marda Complex|41885|6|Mentioned|p144|||Contraction of Marda Calc-Alkaline Complex. see||||||
11264|Marda Complex|42159|5|Briefly described|p317|||||||||
11264|Marda Complex|43097|5|Briefly described|p4|||Rb-Sr isochron age 2630+/-80 Ma.||||||
11264|Marda Complex|43291|5|Briefly described|p2,Fig.2 p3.|||||||||
11264|Marda Complex|43295|6|Mentioned|p2||Archean|age is Rb-Sr 2630+/-80 Ma.||||||07-NOV-08
11264|Marda Complex|43595|5|Briefly described|p226|||Rb-Sr age: 2635+/-80 Ma||||||
11264|Marda Complex|44149|5|Briefly described|p47, p61, p64 Tb.2-5, p68-71|Archean|Archean|See also p74 Tb.2-7, p76. Parent material separated from mantle about 3 Ga. Another age is 2635 +/- 80 Ma (Rb-Sr, Hallberg et al., 1976). Includes stratovolcanoes; calc-alkaline, unlike underlying mafic rocks.|2500 Ma (Fletcher et al., 1984).|||Overlies Diemals Formation (conformably).|Massive porphyritic andesite, overlain by rhyolitic ignimbrite sheets of tuffs and agglomerate; both cut by diorite dykes; then massive granophyric granite forms a high-level intrusion; and finally rhyolite porphyry dykes.|
11264|Marda Complex|50128|5|Briefly described|p32 Fig.2, p34|Archean|Archean|Age: ca 2732 Ma (U-Pb zircon). Geological Province: Yilgarn Craton.||||||19-MAY-14
11264|Marda Complex|60076|6|Mentioned|p15|||Geological Province: Southern Cross Province.||||||
11264|Marda Complex|60460|4|Described|p68, p61, p64, 69-71, 74|||Parent material separated from mantle about 3 Ga.|2635 +/- 80 Ma Rb-Sr  to 2500.|||Overlies Diemals fm (conf).|(5 components) Andesite, Acid ignimbrite/rhyolite/tuff, Diorite dykes intrude 1&2, High-level granitoid/granophyre, Rhyolite porphyry dykes intrude 1-4.|
11264|Marda Complex|61144|5|Briefly described|p13|Archean|Archean|Felsic volcanic and associated epiclastic sedimentary rocks. Geological Province: Southern Cross Province.||||||07-NOV-08
11264|Marda Complex|63778|5|Briefly described|p1125 Fig. 1, p1126 Tb. 1, p1126, p1127|Archaean|Archaean|Age: 2732+/-3, 2734+/-4, 2735+/-7Ma (U-Pb zircon). Geological Province: Yilgarn Craton. Calc-alkaline andesite-dacite-rhyolite rocks. Detailed petrographic and chemistry information is found throughout the text.||||||
11264|Marda Complex|64771|5|Briefly described|p5|Neoarchaean|Neoarchaean|Marda-Diemals greenstone belt, Southern Cross Domain.|2730 Ma.||||Calc-alkaline.|
11264|Marda Complex|65204|6|Mentioned|p7|||Felsic and intermediate extrusive rocks; unconformably overlies a greenstone sequence.||||||
11264|Marda Complex|65265|5|Briefly described|p73, p74 Fig.2, p75|Neoarchean|Neoarchean|Marda-Diemals greenstone belt. Assigned Group status. Butcher Bird Monzogranite, which has been included in the formal stratigraphy of the Complex, is the intrusive equivalent.|Volcanics: c.2732 Ma (GSWA, 2006)||Includes Diemals Formation.||Comprises felsic to intermediate calc-alkaline rocks in which basal conglomerates and sandstones that were derived from the underlying greenstones are overlain by andesite, rhyolite, and rhyolitic ignimbrite.|20-DEC-16
11264|Marda Complex|65269|6|Mentioned|p3 Fig. 1, p24|||S of Diemals Fm, Barlee and Jackson 1:250 000 sheet areas||||||
11264|Marda Complex|65270|5|Briefly described|p3, p21.|Archean|Archean|Southern Cross Granite-Greenstone Terrane, Yilgarn Craton. Emplaced after D1, the first of three deformation events in MARMION and RICHARDSON map areas.|c.2730 Ma (Chen et al. 2003).||||Felsic volcanics.|
11264|Marda Complex|66880|5|Briefly described|p26. |Archean|Archean|Southern Cross Province, central Yilgarn. Arc-related igneous rocks provided these ages.|2732 +/- 3 Ma and 2730 +/- 4 Ma.||||Includes rhyolite and monzogranite.|
11264|Marda Complex|67129|5|Briefly described|p17|Archean|Archean|Southern Cross Domain, Youanmi Terrane.|c.2735 Ma||||Calc-alkaline volcanics.|07-SEP-17
11264|Marda Complex|67198|5|Briefly described|p19, p24|||A greenstone belt in central Yilgarn Craton. The supracrustal sedimentary succession has been dated at 2735 +/- 2 Ma.|c.3130 Ma (Wyche et al., 2004).||||Basal quartzite and muscovite schist.|
11264|Marda Complex|68108|5|Briefly described|p651 Tb.4, p652|Neoarchean|Neoarchean||ca. 2735-2730 Ma; U-Pb (Chen et al. 2003)||||Felsic volcanics; rhyolite-andesite succession.|
11264|Marda Complex|68109|6|Mentioned|p659|Neoarchean|Neoarchean|Marda-Diemals greenstone belt, Southern Cross Domain.|ca. 2732 Ma||||Calc-alkaline.|
11264|Marda Complex|69404|5|Briefly described|p7, p7 Fig.8, p8|Neoarchean|Neoarchean|Southern Cross Domain, Marda-Diemals greenstone belt.|c. 2732 Ma||||Conglomerate, sandstones and siltstone that are conformably overlain by rhyolite, rhyolitic ignimbrite, andesite and subordinate dacite.|
11264|Marda Complex|69583|5|Briefly described|p42|||Marda-Diemals greenstone belt, Southern Cross Domain. Calc-alkaline.|c.2370 Ma.|||||
11264|Marda Complex|70020|5|Briefly described|p117|||Geological province: Yilgarn Craton. Calc-alkaline greenstone assemblage, possibly subduction related (Morris and Kirkland, 2014). Possibly equivalent to mafic volcanics that intruded Norie Group.||||||
11264|Marda Complex|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2734 - 2730 Ma (inferred).||||Felsic volcanic and volcaniclastic rocks; metamorphosed.|
11264|Marda Complex|70273|6|Mentioned|p215|||Marda-Diemals (greenstone) Belt, Southern Cross Domain, Yilgarn Craton. Maximum deformation occurred at c.2730 Ma. Appears also as Marda volcanic complex on the same page.||||||
11264|Marda Complex|70281|5|Briefly described|p454-455|||Chin and Smith (1983). Southern Cross terrane, Yilgarn Craton.|2734 +/- 3 Ma (U-Pb; Nelson, 2001).|||Unconformably overlies Luke Creek succession.|Basal conglomerate, fining upwards into arkoses and siltstones overlain by shallow-water and subaerial andesites, dacites and rhyolites. Metamorphosed to prehnite-pumpellyite facies.|
11264|Marda Complex|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2734-2730 Ma||Includes Butcher Bird Monzogranite.||Felsic volcanic and volcaniclastic rocks; metamorphosed. Sedimentary volcaniclastic rock; metamorphosed.|
11264|Marda Complex|70826|6|Mentioned|p8|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.||||||
11264|Marda Complex|71148|6|Mentioned|p120|||Youanmi Terrane, Yilgarn Craton.||||||
11264|Marda Complex|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Youanmi Terrane.|||Includes Butcher Bird Monzogranite and an unnammed unit.||Felsic volcanic and volcaniclastic rocks; metamorphosed. Sedimentary volcaniclastic rock; metamorphosed.|
11264|Marda Complex|72494|5|Briefly described|p28, p29 Fig.13|||Southern Cross Domain, Yilgarn Craton. Appears as Marda complex on p28.|c.2730 Ma.||||Includes andesite - dacite - rhyolite volcanic rocks.|
11278|Mardie Greensand Member|12471|6|Mentioned|p475 Fig.2, p481.|Early Cretaceous|Early Cretaceous|Oil analyses indicated a mixture of Mesozoic- and Paleozoic-sourced crudes. Biodegraded oil is widespread in this unit in the Robe River Embayment. Mis-spelt (as Madie) on p481. See also Mardie Greensand in this paper.||Unit in Muderong Shale.||Overlies Birdrong Sandstone.||24-OCT-14
11278|Mardie Greensand Member|12491|6|Mentioned|pp458-462.|||Caretta 1 discovered a 41 m gross oil column within poor reservoirs in this unit, and in underlying Barrow Group and Dupuy Formation.||Basal unit in Muderong Shale.||||06-NOV-14
11278|Mardie Greensand Member|23379|4|Described|p160 Fig.2, p158-162,167,171-174|Hauterivian|Valanginian|of Muderong Shale,Barrow Sub-basin.||||||
11278|Mardie Greensand Member|23535|6|Mentioned|p126 Fig 3|||May be equivalent to basal Muderong Shale. Geological Province: Carnarvon Basin.||||||
11278|Mardie Greensand Member|24315|5|Briefly described|p43|Neocomian|Neocomian|Geological Province: Barrow Sub-Basin. Unconformably overlies the Barrow Group. Of the Muderong Shale.||||||09-MAR-05
11278|Mardie Greensand Member|24331|4|Described|p475|Early Cretaceous|Early Cretaceous|See also Mardie Greensand. Of Muderong Shale. Unconformably overlies Flacourt Formation and Barrow Group. Overlain by Muderong Shale. Thickness: 15-40 m. Geological Province: Barrow Sub-basin.||||||21-DEC-04
11278|Mardie Greensand Member|33450|6|Mentioned|Fig.5|||See P11.||||||
11278|Mardie Greensand Member|34840|2|Defined|p73|Neocomian|Neocomian|||||||
11278|Mardie Greensand Member|35144|6|Mentioned|p4|||||||||
11278|Mardie Greensand Member|37320|6|Mentioned|p235|||||||||
11278|Mardie Greensand Member|39486|6|Mentioned|p2092|||||||||
11278|Mardie Greensand Member|41271|3|Fully described|p148|||||||||
11278|Mardie Greensand Member|41439|6|Mentioned|p116|||||||||
11278|Mardie Greensand Member|41440|5|Briefly described|p138|||||||||
11278|Mardie Greensand Member|41709|6|Mentioned|p214|||||||||
11278|Mardie Greensand Member|41732|6|Mentioned|Fig.3|||||||||
11278|Mardie Greensand Member|64973|6|Mentioned|p504|||Misspelt or obsolete name. The original use of the name was not intended to be formal.||||||16-JUN-09
11278|Mardie Greensand Member|67200|5|Briefly described|p8 fig 6, p17 table 1 , p53|Cretaceous|Cretaceous|Thermal conductivity of 1.79 W/mK||Winning Group||Unconformably overlies Flacourt Formation, overlain by Muderong Shale|Parallel bedded, interbedded sandstone and siltstone.|
11278|Mardie Greensand Member|69182|6|Mentioned|Ch3 p30|||||||||
11278|Mardie Greensand Member|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Hauterivian|Valanginian|See also Regional: Fig.6. Northern Carnarvon Basin. Glauconitic. Shortened to Mardie Greensand on p6 and p16. Oil reservoir.||Muderong Shale.||Overlies Birdrong Sandstone.||07-FEB-19
11278|Mardie Greensand Member|70906|5|Briefly described|p757-758|Early Cretaceous|Early Cretaceous|Gorgon Platform. Appears just as Mardie Greensand on p757.||Muderong Shale.||||
11278|Mardie Greensand Member|73564|5|Briefly described|p1225-1226, 1230, 1232|Cretaceous|Cretaceous|Exmouth Sub-basin. Shelfal marine deposits. Appears also as Mardie Greensand.||Muderong Shale.||Overlies Birdrong Sandstone.|Predominantly highly glauconitic sandstone.|
11289|Marell Schist Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
11289|Marell Schist Member|43162|6|Mentioned|6|||||||||
11336|Marlinleigh Sandstone|41271|3|Fully described|p174|||||||||
11353|Marra Mamba Iron Formation|22682|6|Mentioned|p29|||Marra Mamba Supersequence||||||
11353|Marra Mamba Iron Formation|22689|6|Mentioned|137,138 fig 1,141|Paleoproterozoic|Archean|Of Hamersley Group,  Hamersley Basin. SHRIMP age 2597+/-5 Ma. Overlying unit Wittenoom Formation. Also on page 141 fig 2||||||07-NOV-08
11353|Marra Mamba Iron Formation|22701|5|Briefly described|Fig2,p39|Neoarchean|Neoarchean|~2600 Ma. Hamersley Group, Hamersley Basin. Overlies Jeerinah Formation. Overlain by Wittenoom Formation.||||||07-NOV-08
11353|Marra Mamba Iron Formation|23045|5|Briefly described|289|||Age 2597 +/- 5 Ma. Parent Hamersley Group||||||
11353|Marra Mamba Iron Formation|23046|6|Mentioned|183|||||||||
11353|Marra Mamba Iron Formation|23126|5|Briefly described|p381|Proterozoic|Archean|Age: Late Archaean - Early Proterozoic.||||||07-NOV-08
11353|Marra Mamba Iron Formation|23127|5|Briefly described|p375 Fig.1, p377|||||||||
11353|Marra Mamba Iron Formation|23150|5|Briefly described|p24|||of Hamersley Basin.||||||
11353|Marra Mamba Iron Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
11353|Marra Mamba Iron Formation|23354|5|Briefly described|317 Fig.2|||||||||
11353|Marra Mamba Iron Formation|23536|5|Briefly described|Fig 2 p 429|||Also see p 428||||||
11353|Marra Mamba Iron Formation|23570|5|Briefly described|p27|Archean|Archean|Age: 2925+/-5Ma.   Geological Province: Pilbara Craton||||||07-NOV-08
11353|Marra Mamba Iron Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group.||||||07-NOV-08
11353|Marra Mamba Iron Formation|23594|5|Briefly described|p17|||Of Hamersley Group.||||||
11353|Marra Mamba Iron Formation|23598|5|Briefly described|p13|||Of Hamersley Group.||||||
11353|Marra Mamba Iron Formation|23612|5|Briefly described|p840|Archean|Archean|Age: ~2600 Ma.||||||07-NOV-08
11353|Marra Mamba Iron Formation|23746|6|Mentioned|p20|||||||||
11353|Marra Mamba Iron Formation|23808|6|Mentioned|p9|||||||||
11353|Marra Mamba Iron Formation|24025|5|Briefly described|p35|||Of Hamersley Group.  Geological Province: Pilbara Craton.||||||
11353|Marra Mamba Iron Formation|24041|5|Briefly described|p493|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
11353|Marra Mamba Iron Formation|24168|5|Briefly described|p632|||||||||
11353|Marra Mamba Iron Formation|24231|5|Briefly described|p185, p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
11353|Marra Mamba Iron Formation|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Hamersley Group. Overlain by Wittenoom Dolomite. Geological Province: Hamersley Province.||||||07-FEB-11
11353|Marra Mamba Iron Formation|24533|5|Briefly described|p11|Archean|Archean|Of the Hamersley Group. Conformably overlain by Wittenoom Formation; conformably overlies Jeerinah Formation. Chert, banded iron formation, mudstone and siltstone. Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of the Hamersley Group (Mount Bruce Supergroup).  Chert, banded-iron formation, mudstone, and siltstone.  Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Hamersley Group. Overlies Jeerinah Formation. Overlain by Wittenoom Formation. Banded iron-formation. Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton||||||
11353|Marra Mamba Iron Formation|29358|6|Mentioned|p944|||||||||
11353|Marra Mamba Iron Formation|29586|6|Mentioned|p23|||||||||
11353|Marra Mamba Iron Formation|29596|6|Mentioned|Fig.2|||||||||
11353|Marra Mamba Iron Formation|29629|5|Briefly described|p899|||||||||
11353|Marra Mamba Iron Formation|29716|4|Described|Table 1|||||||||
11353|Marra Mamba Iron Formation|29717|6|Mentioned|p1160|||||||||
11353|Marra Mamba Iron Formation|30437|6|Mentioned|p89|||||||||
11353|Marra Mamba Iron Formation|30685|5|Briefly described|p907|||Re mineralization||||||
11353|Marra Mamba Iron Formation|31021|5|Briefly described|p893|||||||||
11353|Marra Mamba Iron Formation|31392|6|Mentioned|p3|||||||||
11353|Marra Mamba Iron Formation|31671|5|Briefly described|p10|||||||||
11353|Marra Mamba Iron Formation|31828|6|Mentioned|p32|||Iron. See also asbestos P41.||||||
11353|Marra Mamba Iron Formation|32326|6|Mentioned|p122|||Hamersley Gp.||||||
11353|Marra Mamba Iron Formation|32389|6|Mentioned|p926|||||||||
11353|Marra Mamba Iron Formation|33538|6|Mentioned|p291|||||||||
11353|Marra Mamba Iron Formation|33540|6|Mentioned|p885|||||||||
11353|Marra Mamba Iron Formation|33542|6|Mentioned|p412|||||||||
11353|Marra Mamba Iron Formation|33544|2|Defined|p82|Precambrian|Precambrian|See also PP83 - 85||||||
11353|Marra Mamba Iron Formation|33687|5|Briefly described|p916|||Also P919 re mineralization||||||
11353|Marra Mamba Iron Formation|34066|4|Described|p5|||L.Prot.||||||
11353|Marra Mamba Iron Formation|34128|6|Mentioned|p17|||See also P18.||||||
11353|Marra Mamba Iron Formation|34129|5|Briefly described|p58|||Proterozoic||||||
11353|Marra Mamba Iron Formation|34135|4|Described|Table 1|||Lower Proterozoic. See also Table 2 & P11||||||
11353|Marra Mamba Iron Formation|34471|6|Mentioned|p22|||||||||
11353|Marra Mamba Iron Formation|34887|6|Mentioned|p19|||||||||
11353|Marra Mamba Iron Formation|35052|6|Mentioned|Fig.2|||||||||
11353|Marra Mamba Iron Formation|35218|6|Mentioned|Fig.1|||||||||
11353|Marra Mamba Iron Formation|35260|6|Mentioned|Fig.4|||Map legend P5.||||||
11353|Marra Mamba Iron Formation|35269|6|Mentioned|p304|||||||||
11353|Marra Mamba Iron Formation|35299|5|Briefly described|p893|||||||||
11353|Marra Mamba Iron Formation|35976|6|Mentioned|Fig.39|||||||||
11353|Marra Mamba Iron Formation|35977|4|Described|p115|||||||||
11353|Marra Mamba Iron Formation|36001|6|Mentioned|p1099|||||||||
11353|Marra Mamba Iron Formation|36247|6|Mentioned|p187|||See also Fig.2.||||||
11353|Marra Mamba Iron Formation|36260|5|Briefly described|p78|Paleoproterozoic|Paleoproterozoic|Contains hematite enrichment ore in the Hamersley Iron Province.  Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|36551|6|Mentioned|Table 23|||||||||
11353|Marra Mamba Iron Formation|36642|6|Mentioned|Table 1|||||||||
11353|Marra Mamba Iron Formation|36882|4|Described|p132|||||||||
11353|Marra Mamba Iron Formation|37170|4|Described|p195|||||||||
11353|Marra Mamba Iron Formation|37223|6|Mentioned|p10|||||||||
11353|Marra Mamba Iron Formation|37297|6|Mentioned|Fig.2|||||||||
11353|Marra Mamba Iron Formation|37460|6|Mentioned|Fig.3.4|||||||||
11353|Marra Mamba Iron Formation|37577|6|Mentioned|p30|||||||||
11353|Marra Mamba Iron Formation|37704|6|Mentioned|p507|||||||||
11353|Marra Mamba Iron Formation|37708|6|Mentioned|p1930|||||||||
11353|Marra Mamba Iron Formation|38776|5|Briefly described|Table 1|||||||||
11353|Marra Mamba Iron Formation|38790|6|Mentioned|p164|||||||||
11353|Marra Mamba Iron Formation|39200|4|Described|p284|||||||||
11353|Marra Mamba Iron Formation|39210|5|Briefly described|Table 1|||||||||
11353|Marra Mamba Iron Formation|39558|6|Mentioned|Table 1|||||||||
11353|Marra Mamba Iron Formation|39589|6|Mentioned|p157|||||||||
11353|Marra Mamba Iron Formation|39697|4|Described|p125|||See also P123||||||
11353|Marra Mamba Iron Formation|40369|6|Mentioned|Plate 1|||||||||
11353|Marra Mamba Iron Formation|40790|6|Mentioned|p195|||||||||
11353|Marra Mamba Iron Formation|40904|6|Mentioned|p86|||||||||
11353|Marra Mamba Iron Formation|40987|6|Mentioned|p51|||||||||
11353|Marra Mamba Iron Formation|41271|6|Mentioned|p175|||||||||
11353|Marra Mamba Iron Formation|41358|6|Mentioned|p144|||||||||
11353|Marra Mamba Iron Formation|41669|4|Described|p27|||||||||
11353|Marra Mamba Iron Formation|41687|4|Described|p87|||||||||
11353|Marra Mamba Iron Formation|41768|4|Described|p27|||||||||
11353|Marra Mamba Iron Formation|42013|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
11353|Marra Mamba Iron Formation|42020|5|Briefly described|p316|||||||||
11353|Marra Mamba Iron Formation|42112|4|Described|p8|||||||||
11353|Marra Mamba Iron Formation|42148|6|Mentioned|p690|||||||||
11353|Marra Mamba Iron Formation|42190|6|Mentioned|p274|||||||||
11353|Marra Mamba Iron Formation|42260|6|Mentioned|p40|||||||||
11353|Marra Mamba Iron Formation|42352|6|Mentioned|p21|||Part equivalent to Lewin Shale of Hickman (1978)||||||
11353|Marra Mamba Iron Formation|42471|5|Briefly described|p7|||Of Hamersley Group.||||||22-APR-09
11353|Marra Mamba Iron Formation|42472|5|Briefly described|Map legend|||||||||
11353|Marra Mamba Iron Formation|42495|6|Mentioned|p2|||||||||
11353|Marra Mamba Iron Formation|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
11353|Marra Mamba Iron Formation|42704|5|Briefly described|Plate 1 and Plate 2E|Proterozoic|Archean|Of the Hamersley Group. Chert, ferruginous chert, BIF, shale.||||||07-NOV-08
11353|Marra Mamba Iron Formation|42730|6|Mentioned|p12|||||||||
11353|Marra Mamba Iron Formation|42743|5|Briefly described|map legend|Archean||||||||07-NOV-08
11353|Marra Mamba Iron Formation|42744|5|Briefly described|p4|||||||||
11353|Marra Mamba Iron Formation|42785|6|Mentioned|Fig.6 P272|||||||||
11353|Marra Mamba Iron Formation|42898|5|Briefly described|p339, Fig.2 p341|||Of Hamersley Group||||||22-APR-09
11353|Marra Mamba Iron Formation|43055|4|Described|p17, Table 4|||Of Hamersley Group.||||||26-NOV-08
11353|Marra Mamba Iron Formation|43063|5|Briefly described|p51|||||||||
11353|Marra Mamba Iron Formation|43119|5|Briefly described|p9|||of Hamersley Group||||||
11353|Marra Mamba Iron Formation|43210|5|Briefly described|Table 1 p3,p4.||Archean|of Hamersley Group.||||||07-NOV-08
11353|Marra Mamba Iron Formation|43262|5|Briefly described|Map Legend||Archean|Of Hamersley Group.||||||22-APR-09
11353|Marra Mamba Iron Formation|43290|5|Briefly described|p6||Archean|Of Hamersley Group.||||||22-APR-09
11353|Marra Mamba Iron Formation|43595|6|Mentioned|Fig.2-49,p220|||||||||
11353|Marra Mamba Iron Formation|44152|4|Described|p169 Fig.2-151, p173, p179 Fig.2-155|||See also p182, p185-187. Removed from Lewin Shale and put into Hamersley Group (MacLeod and de la Hunty, 1966). Detailed comparison of this with similar BIF units of Hamersley Group on p185.||Basal Hamersley Group.|Includes Nammuldi, Mount MacLeod and Mount Newman Members.|Overlies Fortescue Group. Is overlain by Wittenoom Dolomite.|BIF, shale.|
11353|Marra Mamba Iron Formation|44438|14|Not recorded|map legend||Paleoproterozoic|Formation of Hamersley Group. L.Proterozoic.||||||07-NOV-08
11353|Marra Mamba Iron Formation|44477|4|Described|p.10, Table 1||Proterozoic|SF/50-6.||||||
11353|Marra Mamba Iron Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
11353|Marra Mamba Iron Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
11353|Marra Mamba Iron Formation|44501|14|Not recorded|p.6,11,12,17,27,30||Paleoproterozoic|See also table 4,7, for more details. (ref. to MacLeod et al 1963). (F/50-7). Lower Proterozoic.||||||07-NOV-08
11353|Marra Mamba Iron Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11353|Marra Mamba Iron Formation|44503|2|Defined|p.4,6,7,Tb.2, map|||See also p.11-13,17,20,23-25, for more details. Roy Hill Sheet. (F50-12).||||||
11353|Marra Mamba Iron Formation|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
11353|Marra Mamba Iron Formation|44692|2|Defined|p.7,9,11,Tb.1|||See also p.14,20,24-26, for more details. (F50-11).||||||
11353|Marra Mamba Iron Formation|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
11353|Marra Mamba Iron Formation|48755|6|Mentioned|p12|||||||||
11353|Marra Mamba Iron Formation|48760|6|Mentioned|p125|||||||||
11353|Marra Mamba Iron Formation|50131|6|Mentioned|p6 Fig. 4|||Of Hamersley Group. Geological Province: Pilbara Craton.||||||22-APR-09
11353|Marra Mamba Iron Formation|50227|5|Briefly described|p443 Fig. 1|Archean|Archean|Of the Hamersley Group.  Age: 2597Ma.  Geological Province: Hamersley Province.||||||07-FEB-11
11353|Marra Mamba Iron Formation|60373|4|Described|p145 Tb. 1, p148, p150 Tb. 2, p152|Archean|Archean|Of Hamersley Group. Includes; Nammuldi, Mount MacLeod and Mount Newman Members. Overlain by Wittenoom Formation, underlain by Jeerinah Formation. Age: 2597+/-5Ma (SHRIMP).||||||28-OCT-14
11353|Marra Mamba Iron Formation|60706|5|Briefly described|p623|Archean|Archean|Of the Hamersley Group. Includes the Nammulidi, MacLeod and Mount Newman Members. Age: 2597+/-5 Ma. (SHRIMP). Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|61254|6|Mentioned|p257 Fig.1, p258 Fig.2|Neoarchean|Neoarchean|||||||24-APR-20
11353|Marra Mamba Iron Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Hamersley Group. Banded iron-formation, chert, mudstone and siltstone.||||||
11353|Marra Mamba Iron Formation|61575|5|Briefly described|p759|Neoarchean|Neoarchean|Basal unit of Hamersley Group. Bedded chert and and iron-formation. Overlies Jeerinah Formation. Age: 2597+/-5Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
11353|Marra Mamba Iron Formation|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Of the Fortescue Group. Overlies Jeerinah Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
11353|Marra Mamba Iron Formation|61847|5|Briefly described|p295 Fig. 2, p296 Figs. 3 and 4|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton.||||||07-NOV-08
11353|Marra Mamba Iron Formation|62021|6|Mentioned|p169|||||||||
11353|Marra Mamba Iron Formation|62129|3|Fully described|p8, p9, p20, p24, p25|Archaean|Archaean|Of Hamersley Group. Includes Nummuldi, MacLeod and Mount Newman Members. Underlain by Jeerinah Formation conformably. Geological Province: Hamersley Basin.||||||07-FEB-11
11353|Marra Mamba Iron Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Chert, banded iron-formation, and pelite.||||||23-MAR-09
11353|Marra Mamba Iron Formation|63153|5|Briefly described|p1359-1375.|||Hosts the Hope Downs high-grade hematite ore deposits. Typically displays concentric, and less commonly chevron-style, folding.||Basal unit of Hamersley Group.|Includes Nammuldi, MacLeod, Mount Newman Members.|Conformably overlies Jeerinah Formation (Fortescue Group). Is overlain by Wittenoom Formation.|Banded iron formation and shale bands.|
11353|Marra Mamba Iron Formation|63236|5|Briefly described|Map legend|||Geological Province: Hammersley Basin. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||16-JAN-08
11353|Marra Mamba Iron Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Hamersley Group. Geological Province: Hamersley Basin. Chert, banded iron formation, mudstone and siltstone. Age: 2597Ma. Underlies: Wittenoom Formation.||||||07-NOV-08
11353|Marra Mamba Iron Formation|63432|5|Briefly described|p736 Fig. 2, p751|Proterozoic|Proterozoic|||||||07-FEB-11
11353|Marra Mamba Iron Formation|64384|5|Briefly described|p31 Fig. 27, p35 Tb. 6, p36|||Of the Hamersley Group. Comprises Mount Newman, MacLeod and Nammuldi Members. Geological province: Hamersley Basin.||||||07-FEB-11
11353|Marra Mamba Iron Formation|64580|4|Described|map legend||Neoarchean|Of Lower Hamersley Group. Chert, banded iron-formation, mudstone, and siltstone; metamorphosed.||||||09-DEC-08
11353|Marra Mamba Iron Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Age: c. 2597Ma. Geological Province: Pilbara Craton (Hamersley Basin). Banded iron-formation, minor chert, mudstone, and siltstone.||||||
11353|Marra Mamba Iron Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Age: c. 2597Ma.  Geological Province: Hamersley Basin. Banded iron-formation; minor chert, mudstone, and siltstone.||||||26-NOV-08
11353|Marra Mamba Iron Formation|64688|5|Briefly described|Map legend|Archaean|Archaean|Geological province: Hamersley Basin. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||
11353|Marra Mamba Iron Formation|64724|4|Described|p43, p42 Fig. 3|Neoarchean|Neoarchean|Sediments of the Hamersley Basin deposited in a continental passive margin setting.||Of Hamersley Group.||||02-APR-12
11353|Marra Mamba Iron Formation|65194|5|Briefly described|p15 Fig.2.3, p16 Fig.2.4, p100 Fig.2.24|Proterozoic|Proterozoic|Age: Early Proterozoic. Chert and shale; some BIF.||||||
11353|Marra Mamba Iron Formation|65683|4|Described|p799, p800, p801 Fig2, p802-6|||Base of Hamersley Group. Includes Mount Newman, Nammuldi and MacLeod Members. Underlies Wittenoom Formation; conformably overlies Roy Hill Shale Member. Correlated with Lewin Shale. A major iron-ore-bearing horizon; suggested total thickness of 50 m.||||||08-MAR-12
11353|Marra Mamba Iron Formation|65757|6|Mentioned|p81 Tb.2, p84 Fig.2, p85|||Overlies Jeerinah Formation. Overlain by Wittenoom Formation.||||||
11353|Marra Mamba Iron Formation|65825|5|Briefly described|p23.|||||Unit in lower part of Hamersley Group.|||Banded iron-formation.|
11353|Marra Mamba Iron Formation|65829|6|Mentioned|p23.|||Is absent in this map area.||||Overlies Jeerinah Formation. Is overlain by Carawine Dolomite.||
11353|Marra Mamba Iron Formation|66109|6|Mentioned|p191, 195, 197, 199-201, 203|Archean|Archean|Optical photomicrographs and Raman kerogen images of pseudofossils.|~2629 Ma.||||Siltstone, chert, BIF.|
11353|Marra Mamba Iron Formation|66574|5|Briefly described|p921, p928|||Chichester Ranges. Unit in lower Hamersley Group. Contains secondary microplaty hematite within martite-goethite ore.||||||
11353|Marra Mamba Iron Formation|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~2600-~2585 Ma estimated from Fig.11.|||||
11353|Marra Mamba Iron Formation|67025|4|Described|pp318-327.|||230 m thick. Contains much of the iron ore deposits in the Hamersley Group. The natural remanent magnetisation and mean bulk susceptibility of this unit are discussed in this article.||Basal unit in Hamersley Group.||Conformably overlies Jeerinah Formation. Is overlain conformably by Wittenoom Dolomite.|BIF, chert, iron ore.|
11353|Marra Mamba Iron Formation|67056|4|Described|p418 Fig.1, p419 Fig.2, p420 Fig.3(a).|Archean|Archean|Hamersley Province. Has relatively low (c. 0.03 wt%) P.||Basal unit in Hamersley Group.|Includes Nammuldi, MacLeod and Mount Newman Members.|Overlies Fortescue Group. Is overlain by Wittenoom Formation.|Marked by lithological alternations at the metre-scale, known as macrobanding, comprising alternating magnetite-rich mesobanded BIF and non-BIF horizons.|14-MAR-12
11353|Marra Mamba Iron Formation|67130|5|Briefly described|p3 fig 2, p39 fig 36, p40 fig 38|||||Hamersley Group|Includes Nammuldi Member, MacLeod Member, Mount Newman Member|Overlies Jeerinah Formation, Mount Jope Volcanics, overlain by Wittenoom Formation|Banded iron formation|
11353|Marra Mamba Iron Formation|67183|5|Briefly described|p643, p645 Tb.1|Archean|Archean|Here claimed to be the uppermost unit of the Fortescue Group [??] in this region. Present in the Southern Pilbara.||Fortescue Group, Mount Bruce Supergroup||Gradationally overlies the Jeerinah Formation (in the southeast Pilbara).||
11353|Marra Mamba Iron Formation|67201|4|Described|p34, p52-55||||c. 2597 Ma SHRIMP U-Pb Trendall et al. 2004|Hamersley Group|Nammuldi Member, MacLeod Member, Mount Newman Member|Is overlain by Wittenoom Formation, plus Mount Sylvia Formation and Mount McRae Shale.|BIF-dominated.|
11353|Marra Mamba Iron Formation|67827|6|Mentioned|p415, p416 Fig.5 |||Microstructure of iron ores discussed.||Of the Hamersley Group.|Includes Nammuldi Member.|||
11353|Marra Mamba Iron Formation|68035|5|Briefly described|p292, Fig 6|Neoarchean|Neoarchean|Hamersley Basin.||Of Hamersley Group.|Includes Nammuldi Member, MacLeod Member, Mount Newman Member.|Overlies Jeerinah Formation, Fortescue Group. Overlain by Wittenoom Formation.|BIF-dominated.|
11353|Marra Mamba Iron Formation|68056|5|Briefly described|p170-171, 175, 183-185, 188, 190|Archean|Archean|Fe, C isotope data and pyrite shapes tabulated.|c.2598 Ma.|Hamersley Group.||Conformably overlies Jeerinah Formation (Fortescue Group).|BIF, chert.|
11353|Marra Mamba Iron Formation|68280|6|Mentioned|p5, p48, p54, p62||||2600 Ma|Hamersley Group|Includes Mt Newman Member, MacLeod Member, Nammuldi Member|Overlain by Wittenoom Formation, overlies Jeerinah Formation|Banded iron formation.|17-JAN-23
11353|Marra Mamba Iron Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Hamersley Basin.||Of the Hamersley Group.|||Chert, banded iron-formation, mudstone and siltstone; metamorphosed.|06-MAY-14
11353|Marra Mamba Iron Formation|69080|6|Mentioned|p687|||||Basal unit in Hamersley Group.||Conformably overlies Jeerinah Formation (Fortescue Group). Is overlain by Wittenoom Formation.||
11353|Marra Mamba Iron Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Chert, banded iron-formation, mudstone, and siltstone; metamorphosed.|
11353|Marra Mamba Iron Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Chert, banded iron-formation, mudstone, and siltstone; metamorphosed|
11353|Marra Mamba Iron 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 Hamersley Group.|||Chert, banded iron-formation, mudstone, and siltstone; metamorphosed|
11353|Marra Mamba Iron Formation|69538|5|Briefly described|p513-586|Paleoproterozoic|Paleoproterozoic|Abbreviated to MMIF throughout the article. Lesser source of DID (detrital iron deposits) from eroded ferruginised surface BIF.||Unit in Hamersley Group.|Includes Mount Newman, MacLeod and Nammuldi Members.||Includes shallow-water reef limestones in upper part.|27-MAY-16
11353|Marra Mamba Iron Formation|69563|5|Briefly described|p690-691|||Age of upper part of the Formation.|2597 +/- 5 Ma (Trendall et al.,1998).|||||
11353|Marra Mamba Iron Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Hamersley Group.||||
11353|Marra Mamba Iron Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Capricorn Orogen. Of Hamersley Basin; of Aphthalmia Fold Belt. Events: Paterson Orogeny; Miles Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2629-2597 Ma (isotopic; inferred)|Unit of Hamersley Group.|||Chert, banded iron-formation, mudstone, and siltstone; metamorphosed|
11353|Marra Mamba Iron Formation|69739|5|Briefly described|p69-70|||Hamersley Basin.||Hamersley Group.||Overlies Jeerinah Formation (Fortescue Group). Is overlain by Wittenoom Formation.|Iron-oxide dominated. Water-bearing.|
11353|Marra Mamba Iron Formation|69745|6|Mentioned|p269, 274-276|||Crops out in the Mount Wall Fe deposit area, Hamersley Province. See also references to Marra Mamba Formation (p272-273, 278-282, 287).||Hamersley Group.||||
11353|Marra Mamba Iron Formation|70509|5|Briefly described|p14,17,21,25,29-30,34|Neoarchean|Neoarchean|Geological province: Hamersley Province; Pilbara Craton Also referred to as Marra Mamba Formation on p28, and Marra Mamba BIF in text.||Unit of Hamersley Group.||Lowermost unit of Hamersley Group. Overlain by Wittenoom Dolomite. Underlain by Fortescue Group.||
11353|Marra Mamba Iron Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2629-2597 Ma||||Chert, banded iron formation, mudstone and siltstone, metamorphosed.|
11353|Marra Mamba Iron Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||mudstone, chert|
11353|Marra Mamba Iron Formation|71513|6|Mentioned|p66, p87|||Pilbara Craton.||Hamersley Group||Overlain by the Wittenoom Formation, Mt Sylvia Shale and Mt McRae Shale,|Banded-iron formation.|
11353|Marra Mamba Iron Formation|71785|6|Mentioned|p88|||Of Hamersley Gp.||||||
11353|Marra Mamba Iron Formation|71808|4|Described|v-vi, x, p2-p3, p6, p10-|||Hamersley Province. Type exposure is at Wonmunna Gorge. Described in detail in Morris (1991) and Blockley et al (1993); Morris also describes mineralogy and major element geochemistry in detail. Fresh unaltered exposure is relatively rare except in the Weeli Wolli and Alligator Anticlines. See also p11, p13, p19, p21-p22, p30, p38-p39, p47, p52-p54, p65, p77, p81, p85, p87, p90, p92, p102, p105, p117, p127-p129, p149-p150, p156, p215, p238.|||Includes the Nammuldi Member, MacLeod Member, Mount Newman Member, West Angela Member, Paraburdoo Member, Bee Gorge Member.|Conformably overlies the Roy Hill Shale Member. Overlies the Fortescue Group.||
11353|Marra Mamba Iron Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Hamersley Basin.|Max age ~2629, Min age 2597+/-5 Ma.|Hamersley Group, lower|||Chert, banded iron-formation, mudstone, and siltstone; minor carbonate; metamorphosed.|
11353|Marra Mamba Iron Formation|72447|6|Mentioned|p240|||||||||
11353|Marra Mamba Iron Formation|72493|5|Briefly described|p30|||Hamersley Basin.||Basal Hamersley Group.|Nammuldi, McLeod, Mount Newman Members.|Overlies Jeerinah Formation (Fortescue Group). Is overlain by Wittenoom Formation.|Comprises two BIF Members separated by a shale unit.|
11353|Marra Mamba Iron Formation|72569|6|Mentioned|p2|||Of the Hamersley Basin.|||Includes the Mount Newman Member.|||
11353|Marra Mamba Iron Formation|72570|6|Mentioned|p3 fig 1|||||Hamersley Group||||
11353|Marra Mamba Iron Formation|72712|5|Briefly described|p3, p8, p10, p9, p11 Fig 8, p54.|Neoarchean|Neoarchean||c. 2629 Ma to c. 2597 Ma.|Base of Hamersley Group.||Conformably overlies Jeerinah Formation and conformably underlies the Wittenoom Formation.||
11353|Marra Mamba Iron Formation|72758|5|Briefly described|p22-24, p16 Tb.1, p55, 57.|||Comprises 185-230m lowest part of the Hamersley Group. Informally subdivided into 3 subunits, the middle one shale dominated. Crocidolite (blue asbestos) occurs in the upper part of the Marra Mamba Iron Formation in Kungarra Gorge (22deg 48min 00sec S, 116deg 57min 20sec E) Trendall and Blockley (1970). Considered to be the best fibre prospect in the western Hamersley Range.||Hamersley Group||Transitionally or unconformably overlies Jeerinah Formation and conformably underlies Wittenoom Dolomite.|BIF with chert, podded chert, mudstone, and dolomite.|
11353|Marra Mamba Iron Formation|73022|5|Briefly described|p2 Fig.1, p3 Fig.2, p6|||Ferruginous chert and BIF interpreted to record the transition of deposition from distal hydrothermal plumes that are Si-dominated to major transgressions of Fe-rich plumes.||Hamersley Group|Nammuldi Member, MacLeod Member, Mount Newman Member|Overlies the Jeerinah Formation, underlies the Wittenoom Formation.|Banded iron formation overlying a basal ferruginous chert, includes shale.|
11353|Marra Mamba Iron Formation|73290|5|Briefly described|p782-785, 794, 797|||Hamersley Basin.|||Mount Newman Member.|Overlies Jeerinah Formation (Fortescue Group).|Hosts martite-goethite iron ore. Mesobands are either of chert or chert matrix. Fe-rich zones are finely laminated. Textures and petrography described in great detail.|
11353|Marra Mamba Iron Formation|73538|5|Briefly described|p1-2, p4-7|||[Written as Marra Mamba formation on p2].||Hamersley Group|Mount Newman member, MacLeod Member, Nammudi Member|Underlain by the Jeerinah formation of the Fortescue Group. Overlain by the West Angela Member of the Wittenoom Formation.|Includes mudstone/siltstone and iron formation.|
11353|Marra Mamba Iron Formation|73574|5|Briefly described|p763, p770, p771 Fig.6|Proterozoic|Late Archean|||Hamersley Group|||Banded iron Formation.|
11444|Matheson Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Glidden Group.||||||
11444|Matheson Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11444|Matheson Formation|32660|5|Briefly described|Table 6|||||||||
11444|Matheson Formation|32728|5|Briefly described|Table 6|||See also P46||||||
11444|Matheson Formation|36551|6|Mentioned|Table 10|||||||||
11444|Matheson Formation|36885|4|Described|p180|||||||||
11444|Matheson Formation|44155|5|Briefly described|p251 Tb.3-11|||350m thick.||Glidden Group|||Shale, siltstone; minor sandstone.|
11444|Matheson Formation|44231|5|Briefly described|Map Legend||Mesoproterozoic|Of the Glidden Group.  Laminated claystone, dark shale and siltstone, quartz wacke, ferruginous feldspathic sandstone, and quartz sandstone. Geological Province: Glidden Basin.||||||19-MAY-05
11444|Matheson Formation|44397|14|Not recorded|p.15,20, Table 3||Adelaidean|Glidden Group. Defn. on Tech.File E/52-9.||||||
11444|Matheson Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
11444|Matheson Formation|45047|4|Described|p35|||||||||
11444|Matheson Formation|48927|2|Defined|p8|Adelaidean|Adelaidean|||||||
11444|Matheson Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Glidden Group.|||Laminated claystone, fissile laminated commonly micaceous shale and siltstone, flaggy fine and partly pyritic subgreywacke, and ferruginous feldspathic sandstone and medium grained quartz sandstone|
11466|Maude Creek Kimberlite|41158|6|Mentioned|Table 82|||||||||
11466|Maude Creek Kimberlite|69003|5|Briefly described|p5|Neoproterozoic|Neoproterozoic|Kimberley region. Halls Creek Orogen. One of a number of locally diamondiferous lamprophyres and kimberlites intruded around this time.|c.815 Ma.|||||
11466|Maude Creek Kimberlite|69597|6|Mentioned|p5 fig 2b|||||||||
11466|Maude Creek Kimberlite|70731|6|Mentioned|p268|Tonian|Tonian|Geological province: King Leopold Orogen and Lamboo Province, Halls Creek Orogen, Kimberley Craton. Associated with Yampi Orogeny.||||||
11476|Maurice Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
11476|Maurice Formation|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
11476|Maurice Formation|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
11476|Maurice Formation|24301|5|Briefly described|p17|||Geological Province: Amadeus Basin||||||
11476|Maurice Formation|31914|6|Mentioned|p96|||||||||
11476|Maurice Formation|33588|6|Mentioned|p6|||||||||
11476|Maurice Formation|34442|6|Mentioned|p7|||Prot. See also p8. Equiv. Pertatataka Formation.||||||02-NOV-06
11476|Maurice Formation|35102|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|35127|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11476|Maurice Formation|35222|4|Described|Table.2|||||||||
11476|Maurice Formation|35863|6|Mentioned|Table 1|||||||||
11476|Maurice Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11476|Maurice Formation|36551|6|Mentioned|Table 13|||||||||
11476|Maurice Formation|36887|5|Briefly described|p211|||||||||
11476|Maurice Formation|37928|6|Mentioned|Fig.4|||||||||
11476|Maurice Formation|39210|6|Mentioned|Fig.10|||||||||
11476|Maurice Formation|40740|6|Mentioned|p1|||||||||
11476|Maurice Formation|41039|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|41852|6|Mentioned|Table 1|||||||||
11476|Maurice Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, quartzwacke, siltstone.  Geological province: Amadeus Basin.||||||23-JAN-08
11476|Maurice Formation|43503|6|Mentioned|50|||||||||
11476|Maurice Formation|44395|14|Not recorded|p.6,12, Tb.1||Proterozoic|Correlates with Winnall Beds and Pertatataka Formation.||||||
11476|Maurice Formation|44396|5|Briefly described|map legend|||(Proterozoic-Lower Palaeozoic). SF/52-15.||||||
11476|Maurice Formation|44439|2|Defined|p.7,8, Tb.1, map||Neoproterozoic|Upper Proterozoic-Cambrian. Age unclear. Probably equiv.to Cleland Sandstone (Cam.).||||||02-NOV-06
11476|Maurice Formation|44440|14|Not recorded|map legend|Cambrian|Neoproterozoic|Upper Proterozoic-Cambrian.||||||
11476|Maurice Formation|44499|14|Not recorded|opp.p.6, Tb.1|||Proterozoic to Lower Palaeozoic?||||||
11476|Maurice Formation|44500|5|Briefly described|map legend|||Proterozoic to Lower Palaeozoic?||||||
11476|Maurice Formation|45041|4|Described|p38|||Prot. Equiv. Winnall Beds||||||
11476|Maurice Formation|45149|6|Mentioned|Table 1|||Page 17.||||||
11476|Maurice Formation|48842|2|Defined|p.18-20|Early Paleozoic|Neoproterozoic|p.8,15,17-18-20,21-2,27,32,Pl.5,7,8. Tb.I. Overlies Ellis Sandstone and Sir Frederick Conglomerate. U.Prot.-L.Palae.||||||07-NOV-08
11476|Maurice Formation|48864|14|Not recorded|Tb.1,p.10,31,Pl.10|||Cambrian? (G52-2).||||||
11476|Maurice Formation|48963|6|Mentioned|Fig.2|||||||||
11476|Maurice Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red, crossbedded sandstone; siltstone. Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red, cross-bedded sandstone; siltstone.  Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Red, cross bedded sandstone; siltstone. Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
11476|Maurice Formation|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
11476|Maurice Formation|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, quartz greywacke, siltstone. Overlies Sir Frederick Conglomerate and Ellis Sandstone.||||||14-AUG-06
11476|Maurice Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, quartz greywacke, siltstone.||||||
11476|Maurice Formation|64580|4|Described|map legend||Neoproterozoic|Very fine to medium grained quartzose sandstone; cross-bedded; minor laminated, micaceous siltstone.||||||09-DEC-08
11476|Maurice Formation|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
11476|Maurice Formation|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
11476|Maurice Formation|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
11476|Maurice Formation|67326|5|Briefly described|p2, p4, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Sir Frederick Conglomerate and Ellis Sandstone. Is overlain unconformably by Eninta Formation.||
11476|Maurice Formation|67856|4|Described|p340, 338 , 339, 335, 337, 344, 345|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. Type section: Maurice Hills, 23o54'S, 120o18'E. 1800m thick. Deltaic/paralic/shallow marine sediments. No age determination.||||Overlies Ellis Sandstone (conformably) and Sir Frederick Conglomerate (conformably). equivalent to upper part of Winnall beds.|Cross-bedded sandstone, quartz greywacke, micaceous sandstone, clay pellets, heavy mineral concentrations, chocolate-brown laminated siltstone.|
11476|Maurice Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Pertaoorrta Group.||||
11476|Maurice Formation|69003|6|Mentioned|p60|Cambrian|Cambrian|W Amadeus Basin.||||||
11476|Maurice Formation|69031|5|Briefly described|p4, p9|||Amadeus Basin. Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Sir Frederick Conglomerate and Ellis Sandstone.||
11476|Maurice Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Overlies Ellis Sandstone, Mount Currie Conglomerate and Mutitjulu Arkose.||12-JUL-16
11476|Maurice Formation|69438|4|Described|p23:2-4, 18, 20-21, 23|Early Cambrian|Ediacaran|Amadeus Basin. Up to 3600m thick in WA. Alternating fluvial and shallow-marine deposits. Sediments sourced from the S. Was previously considered equivalent to Pertatataka Formation.||Pertaoorrta Group.||Conformably overlies Ellis Sandstone and Sir Frederick Conglomerate. Lateral equivalent of upper parts of Arumbera Sandstone and Winnall beds. Is faulted against Bitter Springs Formation.|Medium- to thinly-bedded, cross-bedded, finely micaceous red sandstone and siltstone.|12-JUL-16
11476|Maurice Formation|69606|5|Briefly described|p1, p4 fig 2, p14, p17|Lower Cambrian|Upper Ediacaran|western Amadeus Basin. Deposited synchronously with the Petermann Orogeny. Potential reservoir and seal rock.||||Overlies the Ellis Sandstone and the Sir Frederick Conglomerate.|Shale, sandstone and siltstone.|
11476|Maurice Formation|69673|6|Mentioned|p64 fig 53, p65, p75|||||||Overlies Sir Frederick Conglomerate, Ellis Sandstone, correlated with Winnall beds||
11476|Maurice Formation|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Top of Winnall Group.||Overlies Ellis Sandstone.||
11476|Maurice 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)||||Lithic and feldspathic sandstone, very fine to medium grained; cross-bedded; minor laminated, micaceous siltstone; commonly silicified|
11476|Maurice Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||21-JAN-22
11476|Maurice Formation|70839|4|Described|p325,329-333,335-340,344|Cambrian|Cambrian|Of Amadeus Basin. Part of Supersequence 4. Reaches up to 3600m thickness in the south, and thins significantly to the north (Haines et al., 2012). Conglomeratic clasts likely derived from Dean Quartzite and Kulail Sandstone, and Tjauwata Group (or Dixon Range beds; WA). SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Two samples, one each from lower and upper parts of the section. Lower Maurice maximum dep age: 831+\-13 Ma (207Pb/206Pb). Upper Maurice maximum dep age: 698+\-20 Ma (207Pb/206Pb). See p332-333 for zircon age spectrums.||||Overlain by Mu Formation. Underlain by Ellis Sandstone and Sir Frederick Conglomerate. Correlable to units 3 and 4 of the Winnall beds.|Immature fluvial sandstone, siltstone, and minor conglomerate. Clasts include quartzite, sandstone, and metasandstone lithologies.|
11476|Maurice Formation|71080|5|Briefly described|p30 fig 21|Cambrian|Cambrian|Amadeus Basin in WA. Supersequence 4.|||||Dominantly sandstone, some shale.|
11476|Maurice Formation|71088|4|Described|p1-p2, p7-p8, p12|Cambrian|Ediacaran|Amadeus Basin. Reassigned to Supersequence 4. Correlated with the Pertatataka Formation by Wells et al., 1970; Grey, 1990 and Lindsay and Korsch., 1991. This unit is very recessive and rarely exposed. This unit reaches a maximum thickness of 3600m exposed in the southern Wallace Hills. Samples dated in this study are described. Max depositional age from detrital zircon from lower Maurice Formation: 831+/-13 Ma. Max depositional age from detrital zircon from upper Maurice Formation: 698+/-20 Ma. See also p14, p16-p22, p24, p33.||||Overlies the Sir Frederick Conglomerate and the Ellis Sandstone. Unconformably overlain by the Mu Formation. Equivalent to the Winnall beds, Angas Hills Formation and Arumbera Sandstone.|Red-brown micaceous siltstone and very friable fine-grained sandstone. Red brown micaceous sandstone, lesser siltstone and local conglomeratic sandstone.|02-MAY-23
11476|Maurice Formation|71114|6|Mentioned|p170 fig 1b|Terreneuvian|Terreneuvian|SW Amadeus Basin.||||||14-FEB-18
11476|Maurice Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
11476|Maurice 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)||||Very fine to medium grained, cross bedded quartz sandstone; minor laminated micaceous siltstone and micaceous sandstone|
11476|Maurice Formation|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
11476|Maurice Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|698+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Medium- to coarse-grained quartz-lithic sandstone.|
11476|Maurice Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Amadeus Basin.||||Overlies the Ellis Sandstone and the Sir Frederick Conglomerate. Overlain by the Mu Formation and Mount Currie Conglomerate.|Lithic sandstone.|
11476|Maurice Formation|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.||||Overlies Ellis Sandstone. Is overlain by Paterson Formation.|Fine- to medium-grained, cross-bedded, poorly-sorted, friable, lithic, feldspathic and micaceous red-brown sandstone; micaceous red-brown siltstone (inferred to have been deposited during the Petermann Orogeny).|
11476|Maurice Formation|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by Sir Frederick Conglomerate or Ellis Sandstone. Grades into Winnall beds.||
11476|Maurice Formation|71842|5|Briefly described|p2-3|Early Cambrian|Early Cambrian|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA).||Unit of Pertaoorrta Group.||Underlain by Sir Frederick Conglomerate or Ellis Sandstone.||
11476|Maurice Formation|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Lithic and feldspathic sandstone, very fine to medium grained; cross-bedded; minor laminated, micaceous siltstone; commonly silicified.|
11476|Maurice Formation|72358|6|Mentioned|p118|Series 2|Series 2|Of Amadeus Basin.||||||
11476|Maurice Formation|72360|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.|||||Red, cross bedded sandstone; siltstone.|09-SEP-19
11476|Maurice Formation|72601|6|Mentioned|p3|Cambrian|Ediacaran|Amadeus Basin, western portion[?].||||||
11476|Maurice Formation|73180|6|Mentioned|p48 Fig.1|Early Cambrian|Early Cambrian|Amadeus Basin.||||Conformably overlies the Mount Currie Conglomerate.||
11484|Maxicar beds|30146|6|Mentioned|p314|||Refers Lowry(1965)||||||
11484|Maxicar beds|44144|6|Mentioned|p504 Tb.4-21|Early Cretaceous|Early Cretaceous|Probably a facies of Donnybrook Sandstone.||||||16-MAY-18
11484|Maxicar beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||claystone, siltstone, sandstone|
11489|May River Shale|40838|6|Mentioned|p279|||||||||
11489|May River Shale|41730|6|Mentioned|Fig.16|||||||||
11489|May River Shale|42860|5|Briefly described|Fig.2|||||||||
11489|May River Shale|43666|6|Mentioned|p47,Table 2|||||||||
11489|May River Shale|67131|5|Briefly described|p2-10|Famennian|Famennian|Presented as "May River Shale". A high-amplitude seismic reflector, prominent within most wells. Associated with a maximum flooding surface (platfrom drowning event). Some controversy over whether this formation belongs to the Fairfield Group or with the underlying latest Famennian reef complex.||Basal Fairfield Group||Said (Fig 2) to be included in Gumhole Formation?|Shale, fine grained, silty limestones, nodular crinoidal-peloidal wackestone-packstone and crinoidal siltstone-wackestone.|03-FEB-20
11489|May River Shale|70492|6|Mentioned|p176, 178|||Lennard Shelf, Canning Basin. Overlies a scalloped, paleokarst surface.||Basal Fairfield Group.||||
11509|McAlly Shale|22496|6|Mentioned|p11||Neoproterozoic|Louisa Downs Group||||||
11509|McAlly Shale|22547|6|Mentioned|p29|||Of Louisa Downs Group.||||||14-NOV-06
11509|McAlly Shale|23383|4|Described|p21, p5 Tb. 5|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group.  Finely laminated mudstone; interbeds of finely laminated siltstone and fine-grained sandstone near base. Conformably overlain by Tean Formation; conformably overlies Yurabi Fm. Max. thickness: 1500 m.  Geol. Prov: Louisa Basin.||||||01-DEC-06
11509|McAlly Shale|23599|4|Described|p18|Neoproterozoic|Neoproterozoic|Age: 568 Ma and 576+/-80 Ma (Rb-Sr). Of Louisa Downs Group. Overlying unit Tean Formation. Underlying unit Yurabi Formation. Geological Province Louisa Basin. Max. thickness: 1500 m.||||||
11509|McAlly Shale|23601|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group. Black, grey and green shale; minor siltstone and fine- to very fine-grained sandstone.||||||25-JAN-05
11509|McAlly Shale|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Louisa Downs Group.||||||
11509|McAlly Shale|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11509|McAlly Shale|32660|5|Briefly described|Table 6|||||||||
11509|McAlly Shale|32728|6|Mentioned|Fig.16|||See also Table 7||||||
11509|McAlly Shale|36888|4|Described|p214|||||||||
11509|McAlly Shale|36898|5|Briefly described|Table IV|||See also Fig.2B||||||
11509|McAlly Shale|37462|6|Mentioned|p294|||||||||
11509|McAlly Shale|38157|6|Mentioned|Table X|||||||||
11509|McAlly Shale|39210|5|Briefly described|p49|||Age||||||
11509|McAlly Shale|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. Probably equivalent to Timperley Shale.||Louisa Downs Group||Conformably overlies Yurabi Formation. Is overlain conformably by Tean Formation.|Black, grey, green siltstone, and shale.|07-MAR-18
11509|McAlly Shale|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Louisa Downs Group.  Black, grey and green shale; minor siltstone and very fine-grained sandstone. Age: <610Ma. Geological Province: Louisa Basin.||||||19-MAY-05
11509|McAlly Shale|44397|14|Not recorded|p.6,22 Table 3||Adelaidean|Defn. on Tech.File E/52-9.||||||
11509|McAlly Shale|44398|14|Not recorded|map legend||Adelaidean|||||||
11509|McAlly Shale|44693|5|Briefly described|Map Legend||Proterozoic|||||||
11509|McAlly Shale|44694|5|Briefly described|Map Legend||Proterozoic|||||||
11509|McAlly Shale|45047|4|Described|p36|||Louisa Downs Group||||||
11509|McAlly Shale|48927|2|Defined|p29|Adelaidean|Adelaidean|||||||
11509|McAlly Shale|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Louisa Downs Group.||||
11509|McAlly Shale|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley.||Of the Louisa Downs Group.||Overlain by the Tean Formation. Underlain by the Yurabi Formation.||
11509|McAlly Shale|67620|5|Briefly described|p2, 5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||Overlies Yurabi Formation. Is overlain by Tean Formation.||
11509|McAlly Shale|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Louisa Downs Group.||||
11509|McAlly Shale|68244|4|Described|p660,665|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region.||Unit of Louisa Downs Group.||Overlain by Tean Formation. Underlain by Yurabi Formation.|Thick monotonous shales|
11509|McAlly Shale|68473|6|Mentioned|p531|||Mount Ramsay. Part of the postglacial succession.||Louisa Downs Group||||
11509|McAlly Shale|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Louisa Basin||Louisa Downs Group|||Black, grey, and green shale; minor siltstone and fine to very fine grained sandstone.|03-AUG-15
11509|McAlly Shale|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Black, grey and green shale; minor siltstone and fine to very fine grained sandstone.|
11509|McAlly Shale|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.|||Black, grey, and green shale; minor siltstone and fine to very fine grained sandstone|
11509|McAlly Shale|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Louisa Downs Group|||Black, grey, and green shale; minor siltstone and fine to very fine grained sandstone|
11509|McAlly Shale|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.|635-541 Ma (biostrat)|Unit of Louisa Downs Group.|||Black, grey, and green shale; minor siltstone and fine to very fine grained sandstone|
11539|McFadden Formation|22589|6|Mentioned|p125||Proterozoic|||||||
11539|McFadden Formation|22716|6|Mentioned|table4, p230||Neoproterozoic|||||||
11539|McFadden Formation|22816|5|Briefly described|p8 Table 1|||Savory Group.||||||11-APR-08
11539|McFadden Formation|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
11539|McFadden Formation|22907|6|Mentioned|41|||Parent Disappointment Group||||||
11539|McFadden Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Officer Basin. ?part of Disappointment Group||||||
11539|McFadden Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Officer Basin.||||||
11539|McFadden Formation|23571|6|Mentioned|p11|||||||||
11539|McFadden Formation|23590|5|Briefly described|p14|||Previously of the now-superseded Savory Group. Of Disappointment Group. Geological Province: Officer Basin.||||||
11539|McFadden Formation|23602|4|Described|p17|||Of Savory Group.||||||
11539|McFadden Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
11539|McFadden Formation|23730|4|Described|p13|Neoproterozoic|Neoproterozoic|Of Disappointment Group. O'lying unit Tchukardine Formation. U'lying unit Mundadjini Formation. Geological Province: Officer Basin. Max. thickness: 1500 m.||||||
11539|McFadden Formation|23760|4|Described|p32|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Geological Province: Officer Basin.||||||
11539|McFadden Formation|24161|6|Mentioned|p16|||||||||
11539|McFadden Formation|24246|5|Briefly described|p17|Proterozoic|Proterozoic|Overlies Boondawarri Formation. Geological Province: Savory Basin.||||||
11539|McFadden Formation|24390|5|Briefly described|p11 Fig. 6|Paleozoic|Neoproterozoic|Geological Province: Officer Basin.||||||07-NOV-08
11539|McFadden Formation|42708|5|Briefly described|Plate 1|Proterozoic||Variation on McFadden Sandstone.||||||
11539|McFadden Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||11-APR-08
11539|McFadden Formation|43492|3|Fully described|9,21|||||||||
11539|McFadden Formation|43756|4|Described|p533,540||Proterozoic|||||||
11539|McFadden Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
11539|McFadden Formation|44111|6|Mentioned|p.58 Fig. 2, p59|||upper Savory Group. May postdate the Paterson Orogeny.||||||
11539|McFadden Formation|50085|5|Briefly described|p11 Fig. 6|Cambrian|Cambrian|Age: <540Ma.  Geological Province: Officer Basin.||||||
11539|McFadden Formation|50205|6|Mentioned|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.||||||
11539|McFadden Formation|61023|5|Briefly described|p15 Fig. 8|Cambrian||Geological Province: Officer Basin.||||||11-APR-08
11539|McFadden Formation|61272|5|Briefly described|p122 Fig.3|||Unconformably overlies the ?Lupton Formation. Unconformably overlain by the ?Table Hill Volcanics.||||||
11539|McFadden Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Ediacaran|Ediacaran|Of the Disappointment Group.  Disconformably or unconformably overlies the Boondawari Formation. Geological Province: Officer Basin. See also p84 and p89 as "McFadden Formation equivalent"||||||07-FEB-11
11539|McFadden Formation|62453|3|Fully described|p5 Fig. 3, 22. 60|Ediacaran|Ediacaran|Geological Province: Officer Basin/Paterson Orogen. Overlies: Boondawarri Formation, Skates Hills Formation, Mundadjini Formation. Underlies unconformably: Durba Sandstone. Sandstone, siltstone and conglomerate.||||||
11539|McFadden Formation|62987|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|Of the Disappointment Group. Overlain by Durba Sandstone. Geological Province: Officer Basin.||||||25-JAN-07
11539|McFadden Formation|64103|6|Mentioned|p400 Fig. 3, p401||Ediacaran|Geological Province: Officer Basin.||||||07-FEB-11
11539|McFadden Formation|64325|5|Briefly described|p82 Fig. 2, p85|Neoproterozoic|Neoproterozoic|Mentioned mostly in terms of equivalents. Age: c.560-545Ma. Geological Province: western Officer Basin.||||||26-AUG-08
11539|McFadden Formation|64580|4|Described|map legend||Neoproterozoic|Of Disappointment Group. Sandstone; minor siltstone and conglomerate.||||||09-DEC-08
11539|McFadden Formation|64772|4|Described|p15, Plate 1  legend|Neoproterozoic|Neoproterozoic|Of Disappointment Gp. Unconformably overlies Skates Hills Fm in S and Boondawari Fm. In N; unconformably overlain by Durba Sandstone. Geological province: Officer Basin. Env. of deposiotion: Eolian dunes.|||||Predominantly of a coarse-grained arenaceous sequence, characterized by laminated to thick-bedded, commonly flaggy, fine- to coarse-grained sandstone, interbedded with similarly bedded feldspathic sandstone and quartz and feldspathic wacke.|25-NOV-13
11539|McFadden Formation|64793|6|Mentioned|p283 fig 2|Ediacaran|Neoproterozoic|Of Officer Basin.||||||
11539|McFadden Formation|64970|5|Briefly described|p718, p719, p719 Fig. 2|Cambrian|Neoproterozoic|Overlian by angular unconformity by Table Hill Volcanics. Geological Province: Officer Basin.||||||27-MAY-09
11539|McFadden Formation|65363|6|Mentioned|p5 Fig.4, p7, p19.|Neoproterozoic|Neoproterozoic|Some rocks named as 'McFadden Formation equivalent' are defined as Lungkarta Formation (Grey et al. in prep. at the time of this report). This unit is remarkably similar to, and in the same relative stratigraphic position as, the eolian sandstone of the Lungkarta Formation.||||||
11539|McFadden Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Northwestern and central Officer Basin||||||
11539|McFadden Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Northwestern and central Officer Basin||||||
11539|McFadden Formation|65410|6|Mentioned|p74.|||Savory Sub-basin. Its stratigraphic position is unclear: Supersequence 3 or 4.||||||
11539|McFadden Formation|65416|4|Described|p137, p138 Fig.3, pp141-144, p146.|Early Cambrian|Ediacaran|Officer Basin. Part of Sequence LP4A of Supersequence LP4. Relationship with the former Babbagoola Formation is discussed in detail. Correlated with Wirrildar beds near the South Australian border, and with the Observatory Hill Formation (eastern Officer Basin). A prograding deltaic sequence.||||Unconformably overlies Steptoe and Browne Formations. Is overlain unconformably by Durba Sandstone, Table Hill Volcanics and Paterson Formation.|Medium- to coarse-grained sandstone, conglomerate lenses and minor siltstone and shale.|
11539|McFadden Formation|65454|4|Described|p7 Fig.3, p11, p30 Fig.A1b|Paleozoic|Cambrian|Of Disappointment Group. Laminated fine- to coarse-grained quartz sandstone, feldspathic sandstone, and quartz wacke; minor conglomerate and siltstone. Similar to Tchukardine and Woora Woora Formations but correlation not clear.||||||21-APR-16
11539|McFadden Formation|67195|5|Briefly described|p10 fig 6, p19 tbl 1, p46, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.47 W/mK. See also App 1, App 2.|||||Grey to tan/grey fine grained sandstone, siltstone; brick red siltstone.|04-JAN-23
11539|McFadden Formation|67200|6|Mentioned|app 2 p10||||||||Fine grained sandstone and siltstone.|
11539|McFadden Formation|67202|5|Briefly described|p64|||NW Officer Basin.||Disappointment Group.||||
11539|McFadden Formation|68270|5|Briefly described|p678,683|Ediacaran|Ediacaran|Western Officer Basin.||||Underlain unconformably by Boondawari Formation.||
11539|McFadden Formation|69003|5|Briefly described|p60, p62|Cambrian|Neoproterozoic|NW Paterson Orogen; NW Officer Basin.||Disappointment Group.||Is overlain by Durba Sandstone.|Red-brown sandstone with giant (60m high) eolian cross-beds.|
11539|McFadden Formation|69029|6|Mentioned|p329|Cambrian|Neoproterozoic|Of Officer Basin.||||Overlain unconformably by Table Hill Volcanics. Underlain unconformably by Wahlgu Formation or Steptoe Formation.||
11539|McFadden Formation|70839|6|Mentioned|p342-343|Early Cambrian|Ediacaran|Of West Officer Basin. Age is broadly constrained between Ediacaran to early Cambrian based on stratigraphic position (Grey et al., 2005).||||||
11539|McFadden Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, siltstone, sandstone|
11539|McFadden Formation|71618|6|Mentioned|p131|||Succession with significant aeolian influence, deposited in response to Paterson-Petermann Orogeny.||||||
11539|McFadden Formation|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Officer Basin.||||Overlies the Wahlgu Formation. Overlain by the Vines Formation and Choorun Formation.|Conglomerate.|
11539|McFadden Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Officer Basin (Phase 1).||Disappointment Group|||Quartz sandstone, commonly giant-scale cross-bedded; minor siltstone and conglomerate; largely eolian.|
11560|McKinrick Hill lamproite|41158|6|Mentioned|p149|||||||||
11582|McWhae Ridge stromatolite|40834|6|Mentioned|Fig.2|||||||||
11608|Meeberrie Gneiss|22694|5|Briefly described|p6|Archean|Archean|||||||07-NOV-08
11608|Meeberrie Gneiss|23569|5|Briefly described|p3|Archean|Archean|Of the Narryer Terrane. Monzogranitic to tonalitic gneiss veined by Eurada Gneiss and Dugel Gneiss. See also p6 Tb. 1.||||||07-NOV-08
11608|Meeberrie Gneiss|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Eurada Gneiss. Underlying unit Weiragoo Granite.||||||07-NOV-08
11608|Meeberrie Gneiss|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Eurada Gneiss. Underlying unit Weiragoo Granite.||||||07-NOV-08
11608|Meeberrie Gneiss|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Eurada Gneiss. Underlying unit Weiragoo Granite.||||||07-NOV-08
11608|Meeberrie Gneiss|23781|4|Described|p12|Archean|Archean|Age: 3730-3620Ma (SHRIMP U-Pb).||||||07-NOV-08
11608|Meeberrie Gneiss|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: 3730-3600 Ma||||||07-NOV-08
11608|Meeberrie Gneiss|24160|5|Briefly described|p64, p66|||Narryer Terrane. Intruded by Dugel Gneiss protoliths. Contains inclusions of Manfred Complex rocks.|3.65 Ga.|Unit in Narryer Gneiss Complex.|||Meta-monzogranite.|
11608|Meeberrie Gneiss|24448|5|Briefly described|p158|Archean|Archean|Age: 3710+/-30 and 3620+/-40Ma (U-Pb).  Geological Province: Yilgarn Craton.||||||07-NOV-08
11608|Meeberrie Gneiss|40588|6|Mentioned|p350|||||||||
11608|Meeberrie Gneiss|41261|3|Fully described|p5|||||||||
11608|Meeberrie Gneiss|42159|5|Briefly described|p310|||See also Fig.1||||||
11608|Meeberrie Gneiss|42800|5|Briefly described|p68|||of Narryer Gneiss Complex||||||
11608|Meeberrie Gneiss|43835|5|Briefly described|Map Legend||Archean|Age: 3730-3600 Ma||||||07-NOV-08
11608|Meeberrie Gneiss|44149|5|Briefly described|p15, p17-25, p30|Eoarchean|Eoarchean|Derived mainly from monzogranite. Other ages given.|3678 +/- 6 Ma (zircon U-Pb; Kinny et al., 1988)|Of Narryer Gneiss Complex||Intruded by Dugel Gneiss.|Quartz-feldspar-biotite gneiss. Amphibolite  or granulite facies metamorphosed.|
11608|Meeberrie Gneiss|50216|5|Briefly described|p203|Archean|Archean|Age: 3650-3620 Ma. Geological Province: Narryer Terrane in northwestern part of Yilgarn Craton.||||||07-NOV-08
11608|Meeberrie Gneiss|62842|5|Briefly described|p203, p217|Archean|Archean|See also the informal Meeberrie gneiss.  Protolith ages of: 3600, 3620, 3670 and 3720Ma.||||||07-NOV-08
11608|Meeberrie Gneiss|64771|5|Briefly described|p7|Eoarchean|Eoarchean|One of the oldest components of Narryer Terrane. SHRIMP U-Pb zircon age.|3730 +/- 10 Ma (Kinny and Nutman, 1996).|||Is intruded by Dugel and Eurada gneisses.|Felsic intrusives; generally migmatitic.|
11608|Meeberrie Gneiss|66299|4|Described|p28.|Archean|Archean|Narryer Terrane, Yilgarn Craton. Contains fragments of Manfred Complex.|Pegmatite c.3730 Ma. Monzogranite 3680-3600 Ma.||||Pegmatite-layered monzogranitic augen gneiss composed of quartz, plagioclase and biotite.|
11608|Meeberrie Gneiss|67129|4|Described|p3, p12|Archean|Archean|Narryer Terrane. Belongs to the tonalite-trondhjemite-granodiorite suite. Is the oldest known rock in Australia. A polyphase migmatite, metamorphosed to granulite facies, with ages ranging 3730-3300 Ma. Also appears as Meeberrie Gneisses on p12.|3731 +/- 14 Ma (SHRIMP)|||Crosscut by Dugel Gneiss.|Gneisses, migmatites: fine- to medium-grained tonalite-granodiorite gneiss cut by coarser grained syenogranite and deformed granites.|07-SEP-17
11608|Meeberrie Gneiss|67855|6|Mentioned|p200 fig 3-3||||3650 Ma|||||
11608|Meeberrie Gneiss|68123|5|Briefly described|p30, 32, 35-38, 41-42|Archean|Archean|Narryer Terrane, Yilgarn Craton. Contains c.3750-3300 Ma zircons. Underwent granulite facies metamorphism between 3730 Ma and 3600 Ma, with another event at c.3300 Ma.||Narryer Gneiss Complex.|Manfred Complex.|Is intruded by Eurada Gneiss and Dugel Gneiss.|A complex migmatite.|
11608|Meeberrie Gneiss|69583|5|Briefly described|p54|||Myers (1988). One of the oldest components of the Narryer Terrane. SHRIMP U-Pb zircon age. Underwent deformation, and amphibolite to granulite facies metamorphism, at c.3300 Ma.|3730 +/- 10 Ma (Kinny and Nutman, 1996).|||Intruded by Dugel and Eurada Gneisses (felsic magma protoliths).|Felsic intrusives, generally migmatitic.|
11608|Meeberrie Gneiss|70020|5|Briefly described|p116|||Geological province: Yilgarn Craton. Sequence of felsic intrusive rocks representing some of the oldest rocks on the Narryer Terrane. Intruded by Dugel and Eurada gneisses. Deformed and metamorphosed between amphibolite and granulite facies.||||||
11608|Meeberrie Gneiss|70826|6|Mentioned|p4|Eoarchean|Eoarchean|Narryer Terrane, Yilgarn Craton.|||||Tonalite-trondhjemite-granodiorite gneiss.|
11608|Meeberrie Gneiss|71168|5|Briefly described|p6|||Narryer and South West Terranes, Yilgarn Craton. A sequence of felsic intrusive rocks.||||Intruded by the Dugel and Eurada Gneisses.||
11608|Meeberrie Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||anorthosite, gabbro, ultramafic schist, felsic gneiss|
11608|Meeberrie Gneiss|71269|5|Briefly described|1m_geologyp12_lut.csv|||Of Narryer Gneiss Complex.|||||Monzogranitic to tonalitic gneiss with gneissic veining. In places contains inclusions of layered anorthosite, leucogabbro, gabbro and ultramafic rocks|
11608|Meeberrie Gneiss|71802|5|Briefly described|p288|||Age groups included 3.73, 3.67. 3.62. 3.60 and 3.30 Ga (Myers and Williams, 1985; Kinney et al., 1988; Kinny and Nutman, 1996).|3730-3300 Ma||||Polyphase migmatite.|
11608|Meeberrie Gneiss|73526|5|Briefly described|p2 Fig.1, p3-4|Eoarchean|Eoarchean|Narryer Terrane, central and eastern. Intruded by fine-grained, foliated granitic sheets in the Mount Narryer region.|3730-3600 Ma||||Composite, upper amphibolite facies quartzofeldspathic gneiss.|
11627|Melligo Sandstone|7433|5|Briefly described|p25 Fig.2, p42, p45. |Aptian|Aptian|Canning Basin. Beach clastics. Thickness from 2 to 20 m. Contains Aptian bivalve Fissilunula clarkei.||||Overlies Broome Sandstone. Is disconformably overlain by Parda Formation, Frezier Sandstone, and by Emeriau Sandstone in far north of the basin.|Beach deposit of well-sorted, planar-laminated, thin-bedded quartzose sandstone containing heavy minerals; most outcrops are silicified.|
11627|Melligo Sandstone|22718|5|Briefly described|P8, Table1 P6||Early Cretaceous|||||||
11627|Melligo Sandstone|22765|5|Briefly described|P10, Table1||Aptian|Maximum thickness is 5m, overlying unit is the Parda Formation.||||||09-DEC-08
11627|Melligo Sandstone|22776|6|Mentioned|p11, Table.3|Early Cretaceous|Aptian|Previously thought to be equivalent to Meda Formation. See also p21.||||||
11627|Melligo Sandstone|23722|4|Described|p36|Cretaceous|Late Jurassic|||||||
11627|Melligo Sandstone|23766|5|Briefly described|p29|Early Cretaceous|Late Jurassic|Parent: Broome Sandstone.||||||01-OCT-08
11627|Melligo Sandstone|30897|5|Briefly described|p16|||||||||
11627|Melligo Sandstone|30898|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
11627|Melligo Sandstone|32648|6|Mentioned|p32|||Lower Cretaceous.||||||
11627|Melligo Sandstone|36224|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||||||01-FEB-05
11627|Melligo Sandstone|36257|6|Mentioned|Table 2.1|||||||||
11627|Melligo Sandstone|36890|3|Fully described|p352|||Formerly Melligo Quartzite.||||||10-FEB-20
11627|Melligo Sandstone|38878|6|Mentioned|Map legend|Aptian|Aptian|||||||
11627|Melligo Sandstone|38886|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11627|Melligo Sandstone|40045|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11627|Melligo Sandstone|40078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11627|Melligo Sandstone|42571|5|Briefly described|Table1 P8|||||||||
11627|Melligo Sandstone|42814|5|Briefly described|p24|||||||||
11627|Melligo Sandstone|42815|5|Briefly described|map|Mesozoic||||||||
11627|Melligo Sandstone|43281|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
11627|Melligo Sandstone|43563|6|Mentioned|Fig2,p5||Early Cretaceous|||||||
11627|Melligo Sandstone|43656|6|Mentioned|Fig.2,p8|Aptian|Barremian|||||||
11627|Melligo Sandstone|43746|6|Mentioned|Fig.2,p11|Aptian|Barremian|||||||
11627|Melligo Sandstone|44143|4|Described|p.431 Table 4-19; p.449, Figure 4-108|Cretaceous|Cretaceous|Up to 20m thick; fine to medium sandstone; beach. Conformably overlies Broome Sandstone; is overlain disconformably by Emeriau and Frezier Sandstones and Parda Formation. Type area at Melligo Creek (PENDER: 16deg 34' S, 122deg 56' E). Contains bivalves, belemnites: Aptian.||||||23-NOV-17
11627|Melligo Sandstone|45153|2|Defined|App.8-132|Aptian|Aptian|Formerly Melligo Quartzite. See also App.6-105||||||
11627|Melligo Sandstone|45158|3|Fully described|p14|||See also p35.||||||10-FEB-20
11627|Melligo Sandstone|61273|5|Briefly described|p85|Early Cretaceous|Early Cretaceous|Fine-grained, thinly bedded, flat to low-angle cross-bedded; contains fossil bivalves. Dimension stone commercially known as Kimberley Sandstone and/or Kimberley Quartzite.||||||
11627|Melligo Sandstone|64449|5|Briefly described|p62 Tb. 2|Early Cretaceous|Early Cretaceous|Consists of laminated to thin bedded, fine to medium sandstone.||||||07-FEB-11
11627|Melligo Sandstone|64580|4|Described|map legend||Early Cretaceous|Fine- to coarse-grained sandstone; minor mudstone and conglomerate.||||||09-DEC-08
11627|Melligo Sandstone|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
11627|Melligo Sandstone|64769|5|Briefly described|p7|Early Cretaceous|Early Cretaceous|Light beige to multicoloured forms displaying prominent liesegang banding over beige-coloured sandy matrix. WA.||||||05-MAY-09
11627|Melligo Sandstone|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
11627|Melligo Sandstone|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Broome Sandstone.||
11627|Melligo Sandstone|68007|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||||25-FEB-20
11627|Melligo Sandstone|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Broome Sandstone.||
11627|Melligo Sandstone|69182|6|Mentioned|Ch4 p9, Ch4 p45,Ch4 p47|Early Cretaceous|Early Cretaceous|North Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.||10-FEB-20
11627|Melligo Sandstone|69297|6|Mentioned|p337, p352|Aptian|Barremian|Broome Platform of the Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Parda Formation.||
11627|Melligo Sandstone|69590|4|Described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
11627|Melligo Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
11627|Melligo Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Early Cretaceous|Early Cretaceous||100-145 Ma||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|10-FEB-20
11627|Melligo Sandstone|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.||10-FEB-20
11627|Melligo Sandstone|71267|4|Described|GEOL_LUT_CSV files|Early Cretaceous|Early Cretaceous|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|145-113 Ma (biostrat)||||Littoral white to pale grey medium to coarse grained silicified quartz sandstone with local large-scale cross bedding. Contains fossil bivalves.|
11627|Melligo Sandstone|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Anketell Formation.|Sandstone.|10-FEB-20
11627|Melligo Sandstone|72034|6|Mentioned|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Shown informally grouped with Mowla and Broome Sandstones. Siliciclastic Canning Basin unit.  Age from biostratigraphy.||||||
11627|Melligo Sandstone|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Fitzroy Trough.||||Overlies Broome Sandstone. Underlies Anketell Formation. Laterally equivalent to Parda Formation.||
11627|Melligo Sandstone|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 Parda Formation.|Dominantly sandstone.|
11629|Mellinjerie Limestone|7433|5|Briefly described|p25 Fig.2, p29, p31 Fig.7. |Middle Devonian|Middle Devonian|Canning Basin. Mainly intertidal and supratidal flats depositional environment.|||||Thin sequence of carbonates and minor evaporites.|
11629|Mellinjerie Limestone|22801|5|Briefly described|P11, Table1 P9||Middle Devonian|||||||
11629|Mellinjerie Limestone|24061|5|Briefly described|p180|||The marine carbonate sediments are now included in the "Lennard River Group".  Geological Province:  Canning Basin.||||||
11629|Mellinjerie Limestone|24062|5|Briefly described|p186 Table 1|Devonian|Devonian|Geological Province: Canning Basin.||||||
11629|Mellinjerie Limestone|30110|6|Mentioned|p81|||||||||
11629|Mellinjerie Limestone|30313|5|Briefly described|p53|||See also p54,55,56,57.||||||13-NOV-07
11629|Mellinjerie Limestone|30595|5|Briefly described|p3|||||||||
11629|Mellinjerie Limestone|31047|5|Briefly described|p344|||Refers earlier use (1967).||||||13-NOV-07
11629|Mellinjerie Limestone|32619|6|Mentioned|p464|||Spores||||||
11629|Mellinjerie Limestone|32648|6|Mentioned|p32|||Mid. U. Dev.||||||
11629|Mellinjerie Limestone|33326|6|Mentioned|p449|||Fauna.||||||
11629|Mellinjerie Limestone|33960|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|33965|4|Described|Table 1|||||||||
11629|Mellinjerie Limestone|33966|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35127|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35201|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35202|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35207|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35222|4|Described|Table.2|||||||||
11629|Mellinjerie Limestone|35223|4|Described|Table.2|||||||||
11629|Mellinjerie Limestone|35225|4|Described|Table 1|||||||||
11629|Mellinjerie Limestone|35226|4|Described|Table 1|||||||||
11629|Mellinjerie Limestone|35250|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35251|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35252|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|35275|6|Mentioned|Fig.5.|||||||||
11629|Mellinjerie Limestone|35497|4|Described|Table 1|||Also on p7.||||||13-NOV-07
11629|Mellinjerie Limestone|35903|4|Described|Table 1|||||||||
11629|Mellinjerie Limestone|36257|6|Mentioned|Table 2.1|||||||||
11629|Mellinjerie Limestone|36438|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|36632|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11629|Mellinjerie Limestone|36890|3|Fully described|p327|||||||||
11629|Mellinjerie Limestone|38878|6|Mentioned|Map legend|Frasnian|Givetian|Givetian - Frasnian||||||
11629|Mellinjerie Limestone|40992|6|Mentioned|Fig.11|||||||||
11629|Mellinjerie Limestone|41276|6|Mentioned|p74|||||||||
11629|Mellinjerie Limestone|42030|5|Briefly described|p746|||see also Fig.2 p744.||||||13-NOV-07
11629|Mellinjerie Limestone|42930|5|Briefly described|Fig.1 p473|Devonian|Devonian|Overlies and interfingers with Poulton Formation; underlies Pillara Limestone. Geological Province: Canning Basin.||||||13-NOV-07
11629|Mellinjerie Limestone|43173|6|Mentioned|54||Late Devonian|||||||
11629|Mellinjerie Limestone|43563|6|Mentioned|Fig.2,p6|Givetian|Eifelian|||||||
11629|Mellinjerie Limestone|43815|6|Mentioned|Table 1,p95-96|||||||||
11629|Mellinjerie Limestone|43818|6|Mentioned|Fig.2.p39||Middle Devonian|||||||
11629|Mellinjerie Limestone|44143|4|Described|p439 Table 4-19, p442, p.443 Fig.4-98|Devonian|Devonian|Up to 300m thick; limestone, dolomite, and shale; shallow marine. Disconformably(?) overlies Tandalgoo Sandstone. Type section between 931 m and 1128m in Sahara 1 (SAHARA: 21deg 04' 40" S, 123deg 23' 30" E). Contains microflora and conodonts: Givetian to Frasnian.||||||23-NOV-17
11629|Mellinjerie Limestone|44356|5|Briefly described|p8,Tb.1 p7|||||||||
11629|Mellinjerie Limestone|45041|6|Mentioned|Fig.45|||M. Devonian||||||
11629|Mellinjerie Limestone|45153|2|Defined|App.3-45|Late Devonian|Late Devonian|See also App.2-28.||||||13-NOV-07
11629|Mellinjerie Limestone|45158|3|Fully described|p26|||||||||
11629|Mellinjerie Limestone|46912|6|Mentioned|Table 1|||Analytical data of Canning Basin cores||||||
11629|Mellinjerie Limestone|46973|6|Mentioned|Fig.17|||||||||
11629|Mellinjerie Limestone|64982|5|Briefly described|p698.|Frasnian|Givetian|Up to 300 m of shallow marine to supratidal deposits containing microflora and conodonts.||||Unconformably overlies Tandalgoo Formation. Is unconformably overlain by Grant Group.|Limestone, minor shales, evaporites and dolomites.|
11629|Mellinjerie Limestone|66949|6|Mentioned|p82-83 Appx.5|Devonian|Devonian|Occurs below 833m in Contention Heights 1 well, and below 1335m in Patience1 well.||||Is overlain by Grant Group.||
11629|Mellinjerie Limestone|67202|6|Mentioned|p44 Fig.2.10|Devonian|Devonian|Canning Basin.||||Unconformably overlain by the Paterson Formation and the Grant Group.||15-FEB-18
11629|Mellinjerie Limestone|68007|5|Briefly described|p6, p10|Devonian|Devonian|Canning Basin. See also reference to Mellinjerie Formation (p4). The type section is in Sahara 1 well, where it overlies ?Clapp Ridge Formation.||||||
11629|Mellinjerie Limestone|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14, Ch4 p30-p35|Middle Devonian|Middle Devonian|Canning Basin. Incorrectly referred to as the Mellinjerie Formation (now obsolete) in Ch4 p9, p13, p14. See also Ch4 p39, Ch4 p42, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p65, Ch4 p74, Ch4 p78, Ch4 p86.||||Overlies the Clapp Ridge Formation.|Shallow marine carbonates.|
11629|Mellinjerie Limestone|69297|6|Mentioned|p337, p352|Frasnian|Givetian|Broome Platform of the Canning Basin.||Shown as ungrouped.||Overlies the Dominic Shale. Overlain by the Clanmeyer Formation.||03-DEC-18
11629|Mellinjerie Limestone|72502|6|Mentioned|p5|Frasnian|Givetian|Broome Platform-Willara Sub-basin, Canning Basin.||||||
11645|Mendena Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11645|Mendena Formation|32660|5|Briefly described|Table 3|||||||||
11645|Mendena Formation|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
11645|Mendena Formation|32728|6|Mentioned|Table 5|||||||||
11645|Mendena Formation|33443|6|Mentioned|p260|||||||||
11645|Mendena Formation|34137|4|Described|Table 1||Carpentarian|Carpentarian. Part of Bastion Group||||||
11645|Mendena Formation|34462|4|Described|Table 1|||Carpentarian||||||
11645|Mendena Formation|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11645|Mendena Formation|36551|6|Mentioned|p27|||||||||
11645|Mendena Formation|36885|4|Described|p185|||||||||
11645|Mendena Formation|44140|5|Briefly described|p294|Paleoproterozoic|Paleoproterozoic|110-150 m thick.||Bastion Group||Conformable on Pentecost Sandstone.|Alternating quartz sandstone and siltstone, dolomite; ripple marks, cross beds.|07-MAR-18
11645|Mendena Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
11645|Mendena Formation|44286|5|Briefly described|Map legend|||||||||
11645|Mendena Formation|44363|5|Briefly described|p.6,12,16,27|||(Carpentarian) Bastion Group.||||||
11645|Mendena Formation|44364|14|Not recorded|map legend|||||||||
11645|Mendena Formation|44366|14|Not recorded|p.16, Table 2||Carpentarian|Part of Bastion Group.||||||
11645|Mendena Formation|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
11645|Mendena Formation|45047|5|Briefly described|p28|||Bastion Group.||||||
11645|Mendena Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Bastion Group.|||Quartz sandstone and green and purple siltstone; fine-grained commonly micaceous and feldspathic sandstone; dolostone|
11645|Mendena Formation|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bastion Basin, North Australian Craton.||Bastion Group.|||Fine- to coarse-grained quartz sandstone, micaceous sandstone, siltstone and mudstone; minor carbonate rock; sandstone contains mudstone pebbles locally.|
11650|Menyous Member|24000|3|Fully described|p349|Devonian|Devonian|Of Pillara Formation.  Max. thickness: 420m.  Geological Province: Canning Basin.||||||
11650|Menyous Member|31870|6|Mentioned|Fig.20|||P128||||||
11650|Menyous Member|40837|6|Mentioned|p264|||||||||
11650|Menyous Member|41215|6|Mentioned|Fig.17|||||||||
11650|Menyous Member|45153|5|Briefly described|App.3-51|||||||||
11667|Mereenie Sandstone|9199|5|Briefly described|Map legend|Devonian|Silurian|White cross-bedded sandstone.  Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|9814|5|Briefly described|Map Legend|Devonian|Devonian|White cross-bedded sandstone.||||||
11667|Mereenie Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Devonian|Late Silurian|Geological province: Amadeus Basin.||||||07-FEB-11
11667|Mereenie Sandstone|22560|5|Briefly described|p3|||Age "mostly" Silurian,  Max and Min limits not specified||||||01-SEP-09
11667|Mereenie Sandstone|22561|4|Described|p22|Devonian|Early Cambrian|||||||
11667|Mereenie Sandstone|22564|4|Described|p60|||Age Siluro-Devonian.  Overlying unit - Pertnjara Group||||||
11667|Mereenie Sandstone|22565|5|Briefly described|p70 & Table 1||Silurian|Thickness at Areyonga Creek measured from surface expression - 700m thick.  Approx. thickness measured from seismic data 710m.||||||
11667|Mereenie Sandstone|22566|4|Described|p84|Early Devonian|Silurian|Of the Larapinta Group.||||||06-NOV-06
11667|Mereenie Sandstone|22646|5|Briefly described|p 107|Devonian|Silurian|Underlain by Harajica and Ooraminna Sandstones in different sections - p107.||||||06-NOV-06
11667|Mereenie Sandstone|22650|4|Described|p 163|Early Devonian||Age of base of Mereenie Sandstone is not known but may be as old as latest Ordovician.||||||
11667|Mereenie Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|||Age Siluro-Devonian.||||||
11667|Mereenie Sandstone|22656|5|Briefly described|p 279|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22760|4|Described|p337|Devonian||Origin - Aeolian Deposition.  Age - Siluro-Devonian.||||||
11667|Mereenie Sandstone|22761|4|Described|p349-350|Early Devonian|Late Ordovician|Age - Mostly Silurian.||||||06-NOV-06
11667|Mereenie Sandstone|22762|5|Briefly described|p369|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22763|5|Briefly described|p394|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|22804|4|Described|p442|||Poorly constrained age but is generally assumed to be Silurian to Early Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|22805|5|Briefly described|p465||Early Devonian|||||||
11667|Mereenie Sandstone|22806|6|Mentioned|Fig 6 on p481|||Age - Ordovician(?)-Devonian(?)||||||
11667|Mereenie Sandstone|22807|6|Mentioned|Fig 3 on p495|Devonian|Silurian|||||||
11667|Mereenie Sandstone|22824|5|Briefly described|p526|||||||||
11667|Mereenie Sandstone|22826|4|Described|p575|Early Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|23361|5|Briefly described|16 Fig.4|Early Devonian|Caradoc|Age: 450-400Ma.||||||06-NOV-06
11667|Mereenie Sandstone|23858|5|Briefly described|p914|Late Ordovician|Late Ordovician|Overlain by Pertnjara Group; underlain by Carmichael Sandstone. Geological Province: Amadeus Basin. Max. thickness: 1500 m.||||||06-NOV-06
11667|Mereenie Sandstone|24063|5|Briefly described|p220|Devonian|Silurian|Geological Province: Amadeus Basin. Maximum thicknes: >900m.||||||
11667|Mereenie Sandstone|24064|5|Briefly described|p229 Fig.7|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|24111|5|Briefly described|p214 Fig. 9|Devonian|Devonian|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||30-MAR-05
11667|Mereenie Sandstone|24301|5|Briefly described|p21|||Unconformably overlies Carmichael Sandstone.  Geological Province: Amadeus Basin||||||06-NOV-06
11667|Mereenie Sandstone|24334|4|Described|p43, p48 Tb.1|Early Devonian|Caradoc|Age: 391 - 458 Ma (?evidence for this precision?).  Overlies the Carmichael Sandstone.  Overlain by the Parke Siltstone.||||||01-SEP-09
11667|Mereenie Sandstone|29474|6|Mentioned|p10|||||||||
11667|Mereenie Sandstone|29591|5|Briefly described|Table 23|||||||||
11667|Mereenie Sandstone|29972|6|Mentioned|p5|||Silurian-Devonian||||||
11667|Mereenie Sandstone|30045|6|Mentioned|p343|||||||||
11667|Mereenie Sandstone|30075|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|30238|4|Described|p64|||Devonian age.||||||06-NOV-06
11667|Mereenie Sandstone|30544|5|Briefly described|p50|||See also p51.||||||06-NOV-06
11667|Mereenie Sandstone|30615|6|Mentioned|p177|||Stratigraphic table - Palm Valley -2||||||
11667|Mereenie Sandstone|30659|6|Mentioned|p89|||Devonian. Palaeomagnetism.||||||
11667|Mereenie Sandstone|30661|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
11667|Mereenie Sandstone|31566|5|Briefly described|p229|||? Silurian - Devonian. See also p230, 231, 233, 239 etc.||||||06-NOV-06
11667|Mereenie Sandstone|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
11667|Mereenie Sandstone|31914|6|Mentioned|p97|||Equivalent? Lennis Sst. & of Wanna Beds.||||||
11667|Mereenie Sandstone|32208|6|Mentioned|Map legend|Devonian|Silurian|Silurian? and Devonian?||||||
11667|Mereenie Sandstone|32619|6|Mentioned|p465|||||||||
11667|Mereenie Sandstone|32648|6|Mentioned|p32|||Sil. - Dev.||||||
11667|Mereenie Sandstone|32865|6|Mentioned|p482|||Partly Dev.||||||
11667|Mereenie Sandstone|33307|6|Mentioned|Fig.6|||||||||
11667|Mereenie Sandstone|33326|6|Mentioned|p449|||||||||
11667|Mereenie Sandstone|33625|6|Mentioned|p185|||Table 2||||||
11667|Mereenie Sandstone|33761|6|Mentioned|p146|||Sil? - Dev.||||||
11667|Mereenie Sandstone|33832|6|Mentioned|p8|||Stratigraphy||||||
11667|Mereenie Sandstone|33844|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|33871|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|33971|6|Mentioned|p34|||Lithology sim. to Crown Pt. Fm.||||||
11667|Mereenie Sandstone|34111|5|Briefly described|p12|||Silurian? - Devonian. See also pp14,16,18.||||||06-NOV-06
11667|Mereenie Sandstone|34433|6|Mentioned|p41|||||||||
11667|Mereenie Sandstone|34442|5|Briefly described|Table 1|||Silurian? - Devonian.||||||06-NOV-06
11667|Mereenie Sandstone|34579|4|Described|Table 2|||Silurian - Devonian. See also pp10,16,17.||||||06-NOV-06
11667|Mereenie Sandstone|35088|6|Mentioned|p98|||||||||
11667|Mereenie Sandstone|35102|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|35223|6|Mentioned|p11|||||||||
11667|Mereenie Sandstone|35997|6|Mentioned|p577|||||||||
11667|Mereenie Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
11667|Mereenie Sandstone|36751|6|Mentioned|p489|||||||||
11667|Mereenie Sandstone|36821|6|Mentioned|p397|||||||||
11667|Mereenie Sandstone|36890|4|Described|p400|||Formerly Mareena Bluff Formation.||||||06-NOV-06
11667|Mereenie Sandstone|37727|4|Described|p72|||See also p14.||||||06-NOV-06
11667|Mereenie Sandstone|37818|6|Mentioned|p81|||||||||
11667|Mereenie Sandstone|38606|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|38885|6|Mentioned|Map legend|Devonian|Devonian|||||||
11667|Mereenie Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
11667|Mereenie Sandstone|39565|6|Mentioned|Fig.14|||||||||
11667|Mereenie Sandstone|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11667|Mereenie Sandstone|40136|6|Mentioned|p36|||||||||
11667|Mereenie Sandstone|40201|5|Briefly described|Table 1|||||||||
11667|Mereenie Sandstone|40387|6|Mentioned|p146|||||||||
11667|Mereenie Sandstone|40642|6|Mentioned|p172|||||||||
11667|Mereenie Sandstone|40740|3|Fully described|p58|||Mention p6.||||||06-NOV-06
11667|Mereenie Sandstone|40810|5|Briefly described|p11|||||||||
11667|Mereenie Sandstone|40834|5|Briefly described|p138|||||||||
11667|Mereenie Sandstone|40906|6|Mentioned|p30|||Mention Fig.11||||||
11667|Mereenie Sandstone|40911|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
11667|Mereenie Sandstone|40926|6|Mentioned|p12|||||||||
11667|Mereenie Sandstone|41018|6|Mentioned|p233|||||||||
11667|Mereenie Sandstone|41039|4|Described|p6|||||||||
11667|Mereenie Sandstone|41190|6|Mentioned|Fig.4|||||||||
11667|Mereenie Sandstone|41224|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41270|6|Mentioned|p270|||||||||
11667|Mereenie Sandstone|41276|6|Mentioned|p61|||||||||
11667|Mereenie Sandstone|41385|6|Mentioned|p363|||||||||
11667|Mereenie Sandstone|41409|6|Mentioned|p290|||||||||
11667|Mereenie Sandstone|41560|6|Mentioned|p551|||||||||
11667|Mereenie Sandstone|41621|5|Briefly described|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41717|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|41723|6|Mentioned|Map legend|Late Ordovician|Early Devonian|||||||
11667|Mereenie Sandstone|41819|6|Mentioned|Map legend|Middle Devonian|Late Ordovician|||||||
11667|Mereenie Sandstone|41820|3|Fully described|p13|||||||||
11667|Mereenie Sandstone|42049|5|Briefly described|p217|||||||||
11667|Mereenie Sandstone|42058|6|Mentioned|p116|||||||||
11667|Mereenie Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
11667|Mereenie Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
11667|Mereenie Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
11667|Mereenie Sandstone|42140|6|Mentioned|p558|||||||||
11667|Mereenie Sandstone|42141|6|Mentioned|p568|||||||||
11667|Mereenie Sandstone|42504|5|Briefly described|p77|||||||||
11667|Mereenie Sandstone|42643|6|Mentioned|p32|||||||||
11667|Mereenie Sandstone|42699|5|Briefly described|map legend|Devonian|Silurian|||||||
11667|Mereenie Sandstone|42776|6|Mentioned|p305|||||||||
11667|Mereenie Sandstone|42940|5|Briefly described|Plate 2|Silurian|Silurian|Sandstone, minor conglomerate.  Age: 440-410Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
11667|Mereenie Sandstone|43035|5|Briefly described|p23|||||||||
11667|Mereenie Sandstone|43105|5|Briefly described|Fig.3,p8.|||||||||
11667|Mereenie Sandstone|43225|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
11667|Mereenie Sandstone|43503|6|Mentioned|11-39|Early Devonian|Silurian|||||||
11667|Mereenie Sandstone|43646|6|Mentioned|Fig.3,p554|Devonian|Silurian|||||||
11667|Mereenie Sandstone|43647|6|Mentioned|p530|||||||||
11667|Mereenie Sandstone|43648|5|Briefly described|Fig.1,p488|||||||||
11667|Mereenie Sandstone|43649|5|Briefly described|fig.1,p454-455,459|||||||||
11667|Mereenie Sandstone|43666|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|43749|6|Mentioned|p37|||||||||
11667|Mereenie Sandstone|43817|5|Briefly described|p61-63|||||||||
11667|Mereenie Sandstone|43869|5|Briefly described|p10|Silurian|Silurian|Wind-blown sand, very porous and stores large quatities of water; main source of groundwater for Alice Springs.  Deposited about 430my ago.||||||06-NOV-06
11667|Mereenie Sandstone|44133|4|Described|p42 Fig. 7.16, 44|Middle Paleozoic|Early Paleozoic|Geological Province: Amadeus Basin. Conformably underlies: Finke Group. May exceed 600m in Thickness in depressions. Conformably overlain by Polly Conglomerate, Langra Formation, Horseshoe Bend Shale.||||||07-NOV-08
11667|Mereenie Sandstone|44158|6|Mentioned|p33|||of Amadeus Basin.||||||
11667|Mereenie Sandstone|44220|14|Not recorded|p.67|||||||||
11667|Mereenie Sandstone|44335|4|Described|p.11|Devonian|Silurian|Table 2. p.10, Sil-Dev.||||||
11667|Mereenie Sandstone|44336|14|Not recorded|map legend|Devonian|Silurian|SG/53-3.  Silurian-Devonian.||||||
11667|Mereenie Sandstone|44342|6|Mentioned|p.5, Table 2|||SG/53-5. ?Silurian-Devonian.||||||
11667|Mereenie Sandstone|44343|14|Not recorded|map legend|Devonian|Silurian|Silurian-Devonian.||||||
11667|Mereenie Sandstone|44393|4|Described|p.3, Tb.1|||||||||
11667|Mereenie Sandstone|44394|14|Not recorded|map legend|||Silurian (?) to Devonian.||||||
11667|Mereenie Sandstone|44395|14|Not recorded|p.9,10,12, Tb.2||Late Ordovician|Upper Ordovician.||||||
11667|Mereenie Sandstone|44396|5|Briefly described|map legend|||(Sil?-Dev). SF/52-15.||||||
11667|Mereenie Sandstone|44402|5|Briefly described|map legend|||Silurian? - Dev.||||||02-DEC-04
11667|Mereenie Sandstone|44433|14|Not recorded|map legend|||Silurian? to Devonian.||||||
11667|Mereenie Sandstone|44439|2|Defined|p.7,8, Tb.1, map|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44440|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44484|14|Not recorded|p.5,8,9,11,Fig.4,Tb1|||(?Sil-Dev). See also p.11,12,14, for more details.||||||
11667|Mereenie Sandstone|44485|14|Not recorded|map legend|||Sil? - Dev.||||||
11667|Mereenie Sandstone|44493|4|Described|p.11, map|Devonian|Ordovician|Bloods Range sheet. (G53-3). Ord-Dev. See p.8,13, for details.||||||
11667|Mereenie Sandstone|44494|14|Not recorded|map legend|Devonian|Ordovician|Ordovician - Devonian.||||||
11667|Mereenie Sandstone|44495|4|Described|p.6, map|Devonian|Ordovician|See p.8-10, Tb.1, for details. (G52-8). Ord-Dev.||||||
11667|Mereenie Sandstone|44497|4|Described|p.11,12, Table 2|Devonian|Ordovician|SF/53-13. Ord-Dev.||||||
11667|Mereenie Sandstone|44498|14|Not recorded|map legend|Devonian|Ordovician|Ordovician-Devonian.||||||
11667|Mereenie Sandstone|44505|14|Not recorded|p.2,4,8,9,Fig 1,Tb.1|Devonian|Silurian|Sil-Dev. See also p.9,12, for more details.||||||
11667|Mereenie Sandstone|44506|14|Not recorded|map legend|||Silurian? to Devion.||||||
11667|Mereenie Sandstone|45036|6|Mentioned|p3|||||||||
11667|Mereenie Sandstone|45041|4|Described|p86|||See also pp87-89. U.Sil.- M.Dev.||||||06-NOV-06
11667|Mereenie Sandstone|45148|6|Mentioned|p20|||||||||
11667|Mereenie Sandstone|45155|6|Mentioned|Fig.8|||||||||
11667|Mereenie Sandstone|45168|6|Mentioned|p6|||||||||
11667|Mereenie Sandstone|45170|6|Mentioned|p8|||||||||
11667|Mereenie Sandstone|46829|6|Mentioned|Fig.2|||||||||
11667|Mereenie Sandstone|46928|6|Mentioned|Table 1|||||||||
11667|Mereenie Sandstone|47050|5|Briefly described|p240|||||||||
11667|Mereenie Sandstone|48639|4|Described|p.4|||See also p.1,5-7,16,Pl.1,Sh.1. ?Ord (Siln-Devn according to B.M.R.) F53-14,G55-2).||||||
11667|Mereenie Sandstone|48838|2|Defined|p.19,22-23, Tb.1|||||||||
11667|Mereenie Sandstone|48842|4|Described|p.20||Paleozoic|p.1,20,27,32,Pl.7. Tb.I.||||||07-NOV-08
11667|Mereenie Sandstone|48862|14|Not recorded|p.1,15,18,25,27-42|||(F52-15). Age uncertain, base at least is Ord. opp.8,9; Pl.4,5,9-11.||||||
11667|Mereenie Sandstone|48863|2|Defined|p.29|||Tb.1. opp.p.7,9,20,28,31,36,37-40,42,Pl.4,9,11,13-14,16. Ordovician-Devonian. (G52-4,G53-1).||||||
11667|Mereenie Sandstone|48864|2|Defined|p.34|Middle Devonian|Early Ordovician|Tb.1. On many pages. p.2,9,10,21,32,35,37,48,50,Pl.10,11,13. L.Ord-Lower or Middle Devonian. (G52-2,3,8).||||||
11667|Mereenie Sandstone|48865|2|Defined|p.4,Fig.26-27|||Many figures. Fig.4,21,25,42,47,51,Fig.14, Pl.8-10. = 'Marena red sandstone'. Upper Ordovician? (G52-8,G53-5).||||||06-NOV-06
11667|Mereenie Sandstone|48880|14|Not recorded|p.20,33,Pl.10,11,13|Devonian|Ordovician|(F53-13,14,G53-3).Ord-Devn.||||||
11667|Mereenie Sandstone|48890|4|Described|p.48, pl.12|Devonian|Silurian|See also Tables, Figs & Plates. Sil-Dev.||||||
11667|Mereenie Sandstone|48963|6|Mentioned|Fig.3|||||||||
11667|Mereenie Sandstone|50098|5|Briefly described|p1||Late Ordovician|Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|50244|6|Mentioned|p100|||||||||
11667|Mereenie Sandstone|60547|5|Briefly described|Map Legend|Devonian|Silurian|White cross-bedded sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|60674|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group.  White to pale brown, fine, well-sorted quartz sandstone.  Geological Province: Amadeus Basin.||||||03-DEC-15
11667|Mereenie Sandstone|61306|5|Briefly described|p14, p40|||High-yielding aquifer rocks. Geological Province: northern Amadeus Basin||||||
11667|Mereenie Sandstone|61309|5|Briefly described|p16 Fig. 4, p25 Fig. 11|||Geological Province: Amadeus Basin.||||||06-FEB-08
11667|Mereenie Sandstone|61385|5|Briefly described|Map legend|Devonian|Silurian|White, crossbedded sandstone.  Geological Province: Amadeus Basin.||||||20-OCT-05
11667|Mereenie Sandstone|61387|5|Briefly described|Map legend|Devonian|Silurian|Of the Pertnjara Group. White sandstone, large-scale cross-bedding.  Geological Province: Amadeus Basin.||||||06-NOV-06
11667|Mereenie Sandstone|61518|5|Briefly described|Map Legend|Devonian|Silurian|White to pale brown fine grained, well sorted quartz sandstone. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|61519|5|Briefly described|Map Legend|Silurian|Silurian|Of the Pertnjara Group. White sandstone, large scale cross bedding. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62376|5|Briefly described|p18|Early Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
11667|Mereenie Sandstone|62379|5|Briefly described|p7 Fig. 2|Devonian|Silurian|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
11667|Mereenie Sandstone|62609|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor conglomerate. Underlies: Pertnjara Group. Overlies: Larapinta Group.||||||14-AUG-06
11667|Mereenie Sandstone|62620|5|Briefly described|Map Legend|Devonian|Silurian|Sandstone, minor  conglomerate.||||||
11667|Mereenie Sandstone|63562|5|Briefly described|p338 fig 3, p352 fig 10, p355|Devonian|Silurian|See also p347 fig 9, p350. Of Amadeus Basin. Up to 1.5 km thick package. Zircons similar to underlying sediments (mostly 0.63-0.49 Ga) thus presumed to be derived from them. Similar age spectrum as Stairway Sandstone.|c.435-405 Ma.|||Overlies Carmichael Sandstone conformably. Overlain by Pertnjara Group unconformably.|Aeolian, lesser fluvial, quartz arenites.|
11667|Mereenie Sandstone|64068|6|Mentioned|p78, 79, p7|Silurian|Silurian|Amadeus Basin. Correlated with Devonian Dulcie Sandstone, Cravens Peak beds, Georgina Basin.||||||
11667|Mereenie Sandstone|64334|5|Briefly described|p39, 42|Silurian|Silurian|Amadeus Basin. Deposition was probably in a foreland basin with highlands to the N.||||Unconformably overlies Carmichael Sandstone (Larapinta Group).|Aeolian, fluvial and locally marginal-marine deposits.|
11667|Mereenie Sandstone|64580|4|Described|map legend|Silurian|Ordovician|Quartz sandstone; minor siltstone; eolian.||||||09-DEC-08
11667|Mereenie Sandstone|64769|6|Mentioned|p29|||Dimension stone from this unit is called Ooraminna Sandstone.||||||06-MAY-09
11667|Mereenie Sandstone|64778|6|Mentioned|p13, 16-17, 20|Silurian|Silurian|Amadeus and Pedirka Basins. Max. palaeotemperature analysis summary.||||||
11667|Mereenie Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10 |Early Devonian|Silurian|Aeolian and fluvial deposition.||||||
11667|Mereenie Sandstone|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
11667|Mereenie Sandstone|65194|6|Mentioned|p30, p57, p59, p67|Paleozoic||Amadeus Basin. Misspelt as Meerenie on p67. Aquifer supplying Alice Springs.||||||
11667|Mereenie Sandstone|65233|4|Described|p3 Fig. 2, p10, p12-13|Early Devonian|Silurian|Of upper Larapinta Group. Gradational with Carmichael Sandstone below. Max.thickness:900m. Geol.prov: Amadeus Basin. Comprises 3 unnamed units - lower aeolian succession overlain by locally developed fluvial deposits, capped by an upper aeolian sandstone.||||||07-FEB-11
11667|Mereenie Sandstone|65272|6|Mentioned|p319, p320 Fig.3|Devonian|Silurian|||||||
11667|Mereenie Sandstone|65342|6|Mentioned|p3, p10.|||Amadeus and Eromanga Basins. Max. thickness at least 338 m.||||Overlies Stairway Sandstone. Is overlain by Pertnjara Group.||
11667|Mereenie Sandstone|65449|5|Briefly described|p34-35|Early Devonian|Late Ordovician|Amadeus Basin. Marginal marine to eolian deposits. Closely resembles Tandalgoo Formation lithologically.||||Time-correlative with Carribuddy Group and Worral Formation.||
11667|Mereenie Sandstone|65489|5|Briefly described|p56, p63-64, p125|Devonian|Devonian|Amadeus Basin. Exhibits particularly good reservoir properties at McDills 1.||||||
11667|Mereenie Sandstone|66767|5|Briefly described|p60|Devonian|Late Ordovician|Amadeus Basin. Up to 1000m thick.||||Overlies Larapinta Group. Is overlain unconformably by Pertnjara Group.|Shallow-marine to fluvial quartz sandstone.|
11667|Mereenie Sandstone|67028|6|Mentioned|p372 Tb. 5|Devonian|Ordovician|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|398-461 Ma magnetic age range|||||24-APR-12
11667|Mereenie Sandstone|67326|5|Briefly described|p2-3|Early Devonian|Silurian|Amadeus Basin.||Larapinta Group.||Overlies Carmichael Sandstone. Is overlain by Parke Siltstone.||
11667|Mereenie Sandstone|67565|5|Briefly described|p5 Fig.3, p42, p47, p52.|||Amadeus Basin. Widespread; occurs as prominent ridges. Shallow marine sands overlain  by aeolian dunes. Thickness from 220-1000 m. Devonian fish remains were recorded from its upper beds. An important aquifer.||||Overlies Carmichael Sandstone. Is overlain by Pertnjara Group.|White to pale brown, fine-grained, well-sorted quartz sandstone.|
11667|Mereenie Sandstone|67856|4|Described|p338 fig 4-30, p347 , 337, 346, 348|Early Devonian|Late Ordovician|Of Wells et al., 1964, 1970 etc. [Database says it is part of Pertnjara Group. This reference says there is unconformity between them] Type section West of Ellery Creek (NT). Shallow marine, eolian, fluviatile. Up to 100 m thick [p346, or 1000m p347]. 9 m exposed in WA.||||Overlies Carmichael Sandstone (unconformably).  Overlain gradationally in some parts and unconformably in others by Pertnjara Group (NT).|White to pale brown, cross-bedded pure quartz sandstone.|
11667|Mereenie Sandstone|68323|6|Mentioned|p4 Fig.2|Early Devonian|Early Devonian|Amadeus Basin.||Larapinta Group.||||
11667|Mereenie Sandstone|69438|3|Fully described|p23:2-5,7,21,32, 36-39, 46-48, 50, 55-57|Late Devonian|Silurian|Pritchard and Quinlan (1962); previously spelled as Mareenie Sandstone (Madigan, 1932). Originally Mereenie Bluff Formation of Chewings (1894) for sandstone at the George Gill Range, Amadeus Basin. Was formerly mapped (Ranford et al., 1965) as including rocks which were subsequently (Wells et al., 1970) assigned as a separate Formation (the Carmichael Sandstone). The type section is in the west MacDonnell Ranges, W of Ellery Creek; reference sections at Stokes Pass and Areyonga Creek further to the W. Up to c.1000m thick. Widespread unit: extends c.800km E-W and c.200km N-S. Is faulted against Carnegie Formation. Is overlain by Brewer Conglomerate unconformably. Age range of Late Ordovician?-Early Devonian? is due to absence of useful fossils. Has been quarried for dimension stone in the Ooraminna area.||Ungrouped.||Overlies Carmichael Sandstone conformably (unconformably in the E), and Pertaoorrta Group unconformably. Is overlain by Parke Siltstone or Hermannsburg Sandstone conformably.|Variably thinly to thickly bedded, white to pale brown very pure quartz sandstone; generally fine-grained, but is occasionally medium-grained, with grains well-rounded and well-sorted. Burrows and arthropod tracks occur.|27-APR-17
11667|Mereenie Sandstone|69439|5|Briefly described|p24:11|Silurian|Ordovician|Amadeus Basin. Possible correlative of Kerridy Sandstone (Ngalia Basin).||||||12-JUL-16
11667|Mereenie Sandstone|69449|5|Briefly described|p34:2 Fig.34.2; 34:5, 7|Devonian|Silurian|Eastern Amadeus Basin, with equivalents in the western Warburton Basin. Potential petroleum reservoir rocks.||||Is overlain by Polly Conglomerate (Finke Group).|Red-brown to orange, fine- to coarse-grained, friable sandstone, cross-bedded and locally calcareous.|12-JUL-16
11667|Mereenie Sandstone|69458|6|Mentioned|p42:8|Early Devonian|Late Ordovician|Amadeus Basin.||||||12-JUL-16
11667|Mereenie Sandstone|69606|5|Briefly described|p3, p4 fig 2|Devonian|Silurian|One outcrop found in WA. Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential reservoir rock.||||Unconformably overlies the Carmichael Sandstone. Unconformably overlain by the Pertnjara Group.|Sandstone.|
11667|Mereenie Sandstone|69673|5|Briefly described|p64 fig 53, p67, p149, p149 fig 120|||1km thick.||||Overlies Carmichael Sandstone, overlain by Parke Siltstone|Fine grained, occasionally medium grained, very pure quartz sandstone.|
11667|Mereenie Sandstone|69982|6|Mentioned|p42|Devonian|Late Ordovician|Amadeus Basin.||||||
11667|Mereenie Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Early Devonian|Silurian|Of Amadeus Basin (Phase 2). Events: Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)||||Quartz sandstone; minor siltstone; largely eolian|
11667|Mereenie Sandstone|70826|6|Mentioned|p7 tbl 3|Devonian|Silurian|Amadeus Basin.||||||24-APR-20
11667|Mereenie Sandstone|71080|6|Mentioned|p30 fig 21|Devonian|Silurian|Amadeus Basin.|||||Dominantly sandstone.|
11667|Mereenie Sandstone|71146|5|Briefly described|p6, p28|Pragian|Ludlow|Amadeus Basin. Hosts trace fossils including burrows, trails, scratch marks and tunnels similar to those found in the Tumblagooda Sandstone.||||Overlies the Carmichael Sandstone (Larapinta Group).|Sandstone.|
11667|Mereenie Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
11667|Mereenie Sandstone|71268|4|Described|GEOL_LUT_CSV files|Early Devonian|Silurian|Geological province: Paterson Orogen. Of Bentley Basin. Events: Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|443.4-393.3 Ma (inferred)|Unit of Pertnjara Group.|||Porous, white to pale-brown, fine grained, well sorted quartz sandstone, minor conglomerate|
11667|Mereenie Sandstone|71279|5|Briefly described|p355 Fig.2,p360,p363-365,p374,p382 Tb.1|Early Devonian|Silurian|Amadeus Basin. Crops out in the Waterhouse Range. Magnetisation described. Modelled magnetic properties.||Larapinta Group.||||
11667|Mereenie Sandstone|71342|6|Mentioned|Ch9 p16, Ch9 p20|||||||Unconformably overlies the Stairway Sandstone. Unconformably overlain by the Finke Group.||
11667|Mereenie Sandstone|71618|6|Mentioned|p130|Devonian|Silurian|Of Amadeus Basin.||||||
11667|Mereenie Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Early Devonian|Silurian|Amadeus Basin (Phase 2).|||||Quartz sandstone; minor siltstone; largely eolian.|
11667|Mereenie Sandstone|72360|5|Briefly described|Map legend|Silurian|Silurian|Of Amadeus Basin.|||||White sandstone, large scale cross bedding.|09-SEP-19
11667|Mereenie Sandstone|72369|4|Described|iii,p3-4-4,34-35,37-40|||Of Amadeus Basin. Widespread in the Amadeus Basin, covering ~800 km east-west and 200 km north-south (Owen in Kennard et al 1986). No previous geochronological analysis, but inferred age constraints provided by c. 480 MA MDA of underlying mereenie Sandstone (Maidment 2005), and paleomagnetic investigation by Li et al. (1991), providing possible Silurian age. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN091 (medium-grained quartz arenite) yielded an interpreted maximum depositional age of 486+\-5 Ma (youngest concordant zircon). This age is within certainty of that provided by Maidment 2005, but inconsistent with paleomagnetic age of Li et al. (1991). Contains Meso- to Neoproterozoic detrital zircon age populations (c. 1235-915 Ma) likely sourced from Musgrave Province. Late Neoproterozoic to Cambrian (c. 750-485 Ma) zircons may have been derived from distal greater Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Archean-Paleoproterozoic grains (c. 3125-1840 Ma) may have been recycled from North Australian Craton. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain by parke Siltstone, or disconformably by Hermannsburg Sandstone. Underlain by Carmichael Sandstone.|Variably thinly- to thickly bedded, white to pale brown, quartz sandstone.|18-DEC-19
11667|Mereenie Sandstone|72374|4|Described|iii,p3-4,20-24,26|||Of Amadeus Basin. Depositional environment: shallow marine in the lower part, becoming aeolian in upper. Paleomagnetic investigation by Li et al 1991 suggested a Silurian (444-419 Ma) age. Provenance studies by Normington et al 2018 indicate recycling of detritus from underlying Amadeus Basin succession, as well as primary sources including Musgrave Province. Sample HB16ND358 (sandstone) yielded an interpreted maximum depositional age of 505+\-5 Ma. Zircons of c. 1300-800 Ma (c. 1209, 1158, 1183 and 1127 Ma peaks) likely derived from Musgrave Province either directly, or recycled from underlying Amadeus Basin succession. Lesser groupings of c. 700-500 Ma and c. 2050-1450 Ma likely sourced directly from Aileron, Warumpi and Musgrave provinces, or recycled from underlying Amadeus Basin succession.||Publication layout suggests this is a unit of Larapinta Group.|||Variably thinly- to thickly bedded, white to pale brown sandstone; well-rounded and well-sorted, fine- to medium-grained quartz arenite.|11-OCT-19
11667|Mereenie Sandstone|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
11667|Mereenie Sandstone|73085|6|Mentioned|p1, p4|early Devonian|Silurian|||Larapinta Group||Underlain by Carmichael Sandstone. Overlain by Parke Siltstone (Pertnjara Group).||
11667|Mereenie Sandstone|73119|5|Briefly described|piii, p1, p21-23, Appendix|Silurian|Silurian[?]|Amadeus Basin, widespread. Depositional environment ranges from shallow marine to fluvial to aeolian. Geochron is new SHRIMP U-Pb detrital zircon maximum depositional age, which is younger than the previous youngest age of 486 +/- 5 Ma (Normington et al., 2018), although still older than the Silurian age proposed using palaeomagnetism (Li et al., 1991). Detrital zircon age components are dominated by Palaeozoic to Neoproterozoic and early Mesoproterozoic zircons with only a small number of older Proterozoic-Archean grains. Sourced dominantly from the Musgrave Province with contributions probably from reworked underlying strata originally sourced from the Aileron and Warumpi provinces. [See article for provenance discussion].|473 +/- 7 Ma SHRIMP U-Pb||||Includes poorly-sorted, medium-grained sandstone.|
11667|Mereenie Sandstone|73279|5|Briefly described|p3, p14|Devonian|Ordovician|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||||Underlain by Larapinta Group [Carmichael Sandstone]. Overlain by Pertnjara Group.|Includes sandstone.|
11667|Mereenie Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
11694|Merlinleigh Sandstone|14228|6|Mentioned|p5 fig 2, p9|Eocene|Eocene|Merlinleigh Sub-basin.||||||
11694|Merlinleigh Sandstone|22814|5|Briefly described|fig2|Cenozoic|Cenozoic|||||||19-NOV-08
11694|Merlinleigh Sandstone|23299|14|Not recorded|p113|||Fossils: Corals.||||||
11694|Merlinleigh Sandstone|23311|5|Briefly described|map legend|Eocene|Eocene|||||||
11694|Merlinleigh Sandstone|23312|5|Briefly described|map legend|Eocene|Eocene|||||||
11694|Merlinleigh Sandstone|23403|4|Described|p9|Eocene|Eocene|||||||24-NOV-09
11694|Merlinleigh Sandstone|23620|5|Briefly described|p4 Fig. 4|Paleogene|Paleogene|||||||07-NOV-08
11694|Merlinleigh Sandstone|23815|4|Described|p301, 302|Late Eocene|Middle Eocene|Geological Province: Carnarvon Basin. Max. thickness: 15 m. Fossiliferous.||||||27-APR-05
11694|Merlinleigh Sandstone|23816|5|Briefly described|p253|Eocene|Eocene|Geological Province: Carnarvon Basin. May correlate to the Victoria Plateau Sandstone.||||||27-APR-05
11694|Merlinleigh Sandstone|23976|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
11694|Merlinleigh Sandstone|23977|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
11694|Merlinleigh Sandstone|23978|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
11694|Merlinleigh Sandstone|24059|5|Briefly described|p147|Eocene|Eocene|Geological Province: Merlinleigh Sub-basin. Maximum thickness: 15m.||||||
11694|Merlinleigh Sandstone|29548|6|Mentioned|p227|||||||||
11694|Merlinleigh Sandstone|31051|6|Mentioned|p83|||||||||
11694|Merlinleigh Sandstone|32648|6|Mentioned|p32|||Eocene||||||
11694|Merlinleigh Sandstone|32750|6|Mentioned|p303|||Eocene. Refers Brunnschweiler (1961)||||||
11694|Merlinleigh Sandstone|35105|6|Mentioned|Fig.5|||See also P81||||||
11694|Merlinleigh Sandstone|35282|6|Mentioned|Fig.2|||||||||
11694|Merlinleigh Sandstone|36257|6|Mentioned|Table 2.1|||||||||
11694|Merlinleigh Sandstone|36293|6|Mentioned|p204|||||||||
11694|Merlinleigh Sandstone|36305|6|Mentioned|p354|||||||||
11694|Merlinleigh Sandstone|36890|3|Fully described|p301|||See also p253.||||||13-SEP-18
11694|Merlinleigh Sandstone|38773|5|Briefly described|p44|||||||||
11694|Merlinleigh Sandstone|40340|6|Mentioned|p15|||||||||
11694|Merlinleigh Sandstone|40617|6|Mentioned|p18|||||||||
11694|Merlinleigh Sandstone|41271|6|Mentioned|p19|||||||||
11694|Merlinleigh Sandstone|41438|6|Mentioned|p111|||||||||
11694|Merlinleigh Sandstone|42116|5|Briefly described|p35|||See also Fig.14||||||
11694|Merlinleigh Sandstone|42473|6|Mentioned|p5|||||||||
11694|Merlinleigh Sandstone|44344|14|Not recorded|p.18,19,opp.4, map|||Dated as ?M.Eocene. (G50-1).||||||
11694|Merlinleigh Sandstone|44345|14|Not recorded|map legend||Eocene|||||||
11694|Merlinleigh Sandstone|44532|4|Described|p.9,10, map|||(G50-5).||||||
11694|Merlinleigh Sandstone|44533|5|Briefly described|map legend||Eocene|Eocene.||||||
11694|Merlinleigh Sandstone|44537|14|Not recorded|map legend||Eocene|||||||
11694|Merlinleigh Sandstone|44657|14|Not recorded|p.5,6,13,14|||(Sandstone).||||||
11694|Merlinleigh Sandstone|45015|5|Briefly described|map legend,  p9|Tertiary|Tertiary|Presented informally on p9 as (Merlinleigh) sandstone. Contains fossils.||||||01-JUN-06
11694|Merlinleigh Sandstone|45016|14|Not recorded|p.92,140|||||||||
11694|Merlinleigh Sandstone|48848|14|Not recorded|p.91|||||||||
11694|Merlinleigh Sandstone|61155|5|Briefly described|p15|Late Eocene|Middle Eocene|Overlies and interfingers with Giralia Calcarenite. Age: 42-38.5Ma. Max. thickness: 15m. Geological Province: Carnarvon Basin.||||||
11694|Merlinleigh Sandstone|61958|5|Briefly described|Map sheet 1|Paleogene|Paleogene|||||||
11694|Merlinleigh Sandstone|67200|5|Briefly described|p8 fig 6, |Eocene|Eocene|||||Overlain by Mandu Limestone|Planar cross bedded pebbly sandstone and siltstone.|
11694|Merlinleigh Sandstone|69011|5|Briefly described|Map Legend|Eocene|Eocene|Southern Carnarvon Basin.|||||Comprises coarse-grained sandstone; lesser siltstone, conglomerate, and claystone; commonly intensely silicified.|
11694|Merlinleigh Sandstone|69182|6|Mentioned|Ch3 p13|Eocene|Eocene|Merlinleigh Sub-basin, Carnarvon Basin.||||||
11694|Merlinleigh Sandstone|70138|5|Briefly described|Map legend.|Eocene|Eocene|Southern Carnarvon Basin.|||||Coarse-grained sandstone; lesser siltstone, conglomerate and claystone; commonly intensely silicified.|
11694|Merlinleigh Sandstone|70795|4|Described|100k_geologyp_lut.csv|Eocene|Eocene|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|41-34 Ma||||Coarse-grained sandstone; lesser siltstone, conglomerate, and claystone; commonly intensely silicified.|
11694|Merlinleigh Sandstone|70826|6|Mentioned|p7 tbl 4|Eocene|Eocene|Northern Carnarvon Basin.||||||
11694|Merlinleigh Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
11694|Merlinleigh Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Eocene|Eocene|Southern Carnarvon Basin.  Age from biostratigraphy.|||||Coarse-grained sandstone; lesser siltstone, conglomerate, and claystone; commonly intensely silicified.|
11698|Merougil Formation|22534|6|Mentioned|Fig.5 p10|||||||||
11698|Merougil Formation|22682|5|Briefly described|p15||Archean|Merougil Supersequence.||||||03-MAR-10
11698|Merougil Formation|42696|6|Mentioned|Plate 1B|Archean||Variation on Merougil Conglomerate, Merougil beds.||||||07-NOV-08
11698|Merougil Formation|42870|5|Briefly described|Table 1, P67|||||||||
11698|Merougil Formation|60514|4|Described|p25 Fig. 2, p26 Fig. 3, p27 Fig. 4, p30|Archean|Archean|Unconformably overlies the Black Flag Group. Age: 2664+/-6 Ma. Composed of lensoidal, monomictic to increasingly polymictic conglomerate units, and massive to stratified sandstones.Geological Province: Yilgarn Craton.||||||07-FEB-11
11698|Merougil Formation|60623|4|Described|p25 Fig.2|Archean|Archean|Age: 2664+/-6 Ma. Unconformably overlies Black Flag Group. Conglomerate and sandstones. Interpreted as a braided river system. Geological Province: Eastern Goldfields.||||||07-NOV-08
11698|Merougil Formation|62097|6|Mentioned|p310|Archean|Archean|Geological Province: Kalgoorlie Terrane in Eastern Godlfields Superterrane of the Yilgarn Craton.||||||07-NOV-08
11698|Merougil Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|SE Kambalda Domain. Merougil Sequence.|||||Fluvial sequences.|
11698|Merougil Formation|68289|6|Mentioned|p15, p29|||Kambalda area. See also the Merougil Conglomerate.||||Equivalent to the Navajo Sandstone.||
11698|Merougil Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||biotite-bearing pebbly sandstone, sandstone, and siltstone; metamorphosed|
11698|Merougil Formation|69631|5|Briefly described|p18, p20|||Kambalda area. Interpreted as a high-discharge deposit in an area of high relief, likely to have formed a braid-plain; alternatively, a rapidly reworked pyroclastic deposit.||||Correlated with Navajo Sandstone.|Coarse-grained, quartz-rich sandstone; basal conglomerate.|
11698|Merougil Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2664 +/- 6 Ma (isotopic) - 2640 Ma (inferred).||||Biotite-bearing pebbly sandstone, sandstone, and siltstone; minor polymictic conglomerate; metamorphosed.|
11698|Merougil 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).|2664+\-6 Ma; 2640 Ma (inferred)||||Biotite-bearing pebbly sandstone, sandstone, and siltstone; metamorphosed|
11698|Merougil Formation|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2664+/-6 - 2640 Ma||||Biotite bearing pebbly sandstone, sandstone and siltstone; metamorphosed. Minor polymictic conglomerate; metamorphosed.|
11698|Merougil Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton undivided events.|2664+\-6 Ma; 2640 Ma||||Biotite-bearing pebbly sandstone, sandstone, and siltstone; metamorphosed|
11698|Merougil 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). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2664+\-6 Ma; 2640 Ma||||Biotite-bearing pebbly sandstone, sandstone, and siltstone; minor polymictic conglomerate; metamorphosed|
11698|Merougil Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||Max age 2664+/-6 Ma, min ~2640 Ma.||||Biotite-bearing pebbly sandstone, sandstone, and siltstone; minor polymictic conglomerate; metamorphosed.|
11698|Merougil Formation|72095|6|Mentioned|p6, p8|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton.|<2664 Ma|||||
11698|Merougil Formation|73238|5|Briefly described|p3, 4-5, 12, 18, 20|||St Ives, Kambalda district, Eastern Goldfields Terrane.|2664 +/- 6 Ma (Squire et al., 2010).|||Unconformably overlies Kalgoorlie Sequence.||
11698|Merougil Formation|73391|6|Mentioned|p19, 21, 99, 304|||Kambalda area. Similar age and character to Kurrawang Formation in Kalgoorlie Terrane.||||||
11698|Merougil Formation|73453|6|Mentioned|p2|||||||||
11698|Merougil Formation|73596|6|Mentioned|p1160-1162|Neoarchean|Neoarchean|Kalgoorlie-Kambalda area, Kalgoorlie Terrane.|2664 +/- 6 Ma (MDA).|||Overlies Gidji Lake Formation (Black Flag Group). Is overlain by Kurrawang Formation.||
11737|Mertondale Granite|35113|6|Mentioned|p32|||See also P52.||||||
11753|Mianwali Formation|30565|6|Mentioned|p117|||||||||
11753|Mianwali Formation|32164|6|Mentioned|p488|||||||||
11753|Mianwali Formation|34008|6|Mentioned|p69|||See also P75||||||
11769|Michael Hills Gabbro|30386|5|Briefly described|p14|||||||||
11769|Michael Hills Gabbro|30390|4|Described|p138|||See also P139-145||||||
11769|Michael Hills Gabbro|35726|6|Mentioned|p102|||||||||
11769|Michael Hills Gabbro|36551|6|Mentioned|p115|||||||||
11769|Michael Hills Gabbro|36886|3|Fully described|p203|||||||||
11769|Michael Hills Gabbro|42325|5|Briefly described|p6|||||||||
11769|Michael Hills Gabbro|43609|6|Mentioned|Fig.13,p14|||||||||
11769|Michael Hills Gabbro|44139|5|Briefly described|p284, p285 Fig. 3-69|||Of Giles Complex. 6400m sequence of gabbro, anorthosite, pyroxenite.|| ||||10-SEP-12
11769|Michael Hills Gabbro|49833|4|Described|p13|||||||||
11769|Michael Hills Gabbro|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Giles Complex.||||||
11834|Milesia Formation|30388|4|Described|Table 1|||Middle Proterozoic age. Mission Group||||||
11834|Milesia Formation|30390|5|Briefly described|p81|||||||||
11834|Milesia Formation|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11834|Milesia Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11834|Milesia Formation|33478|6|Mentioned|p452|||||||||
11834|Milesia Formation|35308|6|Mentioned|p452|||||||||
11834|Milesia Formation|36551|6|Mentioned|p22|||See also Table 31.||||||
11834|Milesia Formation|36886|4|Described|p198|||||||||
11834|Milesia Formation|39120|6|Mentioned|p146|||||||||
11834|Milesia Formation|40309|6|Mentioned|p91|||||||||
11834|Milesia Formation|67375|5|Briefly described|p38 Table 1, p52-53, 299.|Mesoproterozoic|Mesoproterozoic|Maximum age from Thomas Rhyolite within underlying Cassidy Group. Minimum age from Bitter Springs Formation which overlies the equivalent of the overlying Townsend Formation, in the Amadeus basin.|Between 1057 +/- 6 Ma and 825-800 Ma.|Unit in Mission Group.||Overlies Lilian Formation. Is overlain by Townsend Quartzite.|Basalts; commonly highly altered; strongly amygdaloidal or quartz-mottled; autoc;lastic or peperitic breccias with sandstone infills; pinkish quartzitic sandstone and conglomerate intercalations; local red-bed type arkosic sandstone.|12-SEP-18
11834|Milesia Formation|67553|4|Described|p40,53-54,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Minimum thickness: 300m. Uppermost continental redbeds is transitional to the overlying Townsend Quartzite.||Unit of Mission Group.||Uppermost unit of Mission Group. Overlain by Townsend Quartzite. Underlain by Lilian Formation.|Basaltic lava flow: highly altered, strongly amygdaloidal or quartz-mottled basalt, basalt breccia, sedimentary intercalations include pinkish, quartzitic sandstones, and conglomerates, and uppermost continental red beds.|
11834|Milesia Formation|68995|5|Briefly described|p10, p19, p20|Stenian|Stenian|Minimum thickness of around 300m.||Mission Group||Overlain by the Townsend Quartzite.|Basaltic volcanic rocks that are commonly highly altered, strongly amygdaloidal or strongly quartz mottled. Basalts are overlain by ferruginous, fine to coarse-grained and possibly subarkosic, sandstone.|
11834|Milesia Formation|69091|5|Briefly described|p75|||Upper part of Mission Group.||Mission Group|||Basalt dominated.|
11834|Milesia Formation|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mission Group|||Meta-basalt, basalt and basaltic andesite; minor interlayered sandstone and conglomerate, epidotized; sandstone; minor beds with rare rounded pebbles to 5 cm, and conglomerate units with rounded pebbles to 10 cm; quartzite|
11834|Milesia Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Six facies are mapped separately.||Mission Group.||Overlies Lilian Formation. Is overlain by Townsend Quartzite.|Granule and pebble conglomerates; red sandstones; basalt and basaltic andesite, strongly vesicular and amygdaloidal, with well-developed autoclastic brecciation including peperite; minor interlayered sandstone and conglomerate, epidotised.|
11834|Milesia Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1040 Ma - 1057 Ma (Inferred)|Mission Group|||Basalt and basaltic andesite, conglomerate with subangular to subrounded granules, poorly sorted fine-coarse grained sandstone interbedded with pebble conglomerate; interlayered ripple bedded sandstone pebble conglomerate and amygdaloidal basalt.|
11834|Milesia 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, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Basalt and basaltic andesite; strongly vesicular and amygdaloidal; laminated sandstone with Fe staining interlayered with pebble conglomerate.|
11834|Milesia Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, quartzite, greywacke, basalt|
11834|Milesia 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, 1m_geologyp12_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Basalt and basaltic andesite; strongly vesicular and amygdaloidal; coarse-grained red sandstone, conglomerate, fine-grained laminated sandstone with pervasive Fe-staining.|
11844|Miller Basalt|30388|4|Described|Table 1|||Table 1 on P9-10. Middle Proterozoic age. Cassidy Group||||||
11844|Miller Basalt|30390|4|Described|p76|||See also P77||||||
11844|Miller Basalt|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Cassidy Group||||||
11844|Miller Basalt|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11844|Miller Basalt|36551|6|Mentioned|Table 31|||||||||
11844|Miller Basalt|36886|4|Described|p198|||||||||
11844|Miller Basalt|67375|4|Described|p38 Table 1, p49. |Mesoproterozoic|Mesoproterozoic|Total thickness about 750 m. Contains conspicuous, resistant, orange-weathering cherty mudstone-sandstone layers near the base; and a mappable, 200-250m wide zone near the middle with sandstones and conglomerates.|Between 1065 +/- 5 Ma and 1057 +/- 6 ma.|Topmost unit in Cassidy Group.||Overlies Hilda Rhyolite. Is overlain by Frank Scott Formation of the Mission Group.|Lava flows with 10-20m thick basal sequences of massive basalts that grade upward into progressively stronger vesicular and amygdaloidal basalts; locally with brecciated tops; mudstone-sandstone, volcaniclastic conglomerate, cherty microbialites.|
11844|Miller Basalt|67553|4|Described|p40,51-53,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. A repetitive succession of lava flows characterised by 10-20 m thick basal sequences of massive basalts grading upward into progressively stronger vesicular and amygdaloidal basalts. Also includes substantial amount of sedimentary interlayers and horizons. Basal 1-2m thick cherty to quartzitic mudstone-sandstone layers (containing redistributed rhyolitic ash?) form a laterally traceable marker interval within the Miller Basalt.||Unit of Cassidy Group.||Uppermost unit of Cassidy Group. Overlain by Frank Scott Formation or Gamminah Conglomerate/Mission Group. Underlain by Hilda Rhyolite.|Repetitive sequence of upward-grading, massive to vesicular and amygdaloidal basalts, intercalated with volcaniclastic conglomerates and sandstones, cherty-epidotitic mudstones, fine-grained cherty microbialites, siltstones, sandstones.|
11844|Miller Basalt|68995|5|Briefly described|p7 Fig.3, p9 Tb.1, p18-19, p49 Fig.25|Stenian|Stenian|Estimated 720m thick.||Cassidy Group||Overlies the Hilda Rhyolite. Overlain by the Frank Scott Formation or the Gamminah Conglomerate.|Massive basalts that grade upwards into vesicular and amygdaloidal basalts. In places there are intensively silicified or brecciated basalts, marking the top of basalt flows. Basalts are intercalated with sandstones and volcaniclastic conglomerates.|
11844|Miller Basalt|69091|6|Mentioned|71 Fig.4.14|||||Cassidy Group||||
11844|Miller Basalt|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample descriptions include: metasedimentary rock; metaconglomerate; metabasalt. Mentioned in GEOCHRON/174691.1.pdf and 174690.1.pdf.||Cassidy Group|||Basalt and basaltic andesite; minor quartz-rich mudstone to sandstone interbeds, epidotized; interlayered massive to vesicular and amygdaloidal basalt and basaltic andesite, and volcanolithic conglomerate and sandstone.|
11844|Miller Basalt|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
11844|Miller Basalt|70095|5|Briefly described|p16-17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of basaltic package: 0.5km.||Unit of Cassidy Group.||Uppermost unit of Cassidy Group. Overlain by Mission Group. Underlain by Hilda Rhyolite.||
11844|Miller Basalt|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. A sub-unit, of interlayered massive to vesicular and amygdaloidal basalt and basaltic andesite with volcanolithic conglomerate and sandstone, is mapped separately.||Cassidy Group.||Overlies Hilda Rhyolite. Is overlain by Frank Scott Formation.|Basalt and basaltic andesite with vesicular and amygdaloidal flow tops and local flow-top breccia; minor quartz-rich mudstone to sandstone interbeds; epidotised.|
11844|Miller Basalt|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Cassidy Group|||Massive-vesicular and amygdaloidal basalt and basaltic andesite, with vesicular and amygdaloidal flow tops and local flow-top breccia; volcanolithic conglomerate, sandstone and minor quartz-rich mudstone interbeds; epidotized.|
11844|Miller Basalt|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.|||Basalt and basaltic andesite, with vesicular and amygdaloidal flow tops and local flow-top breccia; minor quartz-rich mudstone to sandstone interbeds; epidotized|
11844|Miller Basalt|71211|6|Mentioned|p216|||||Cassidy Group||||
11844|Miller 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). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Basalt and basaltic andesite, with vesicular and amygdaloidal flow tops and local flow-top breccia; minor quartz-rich mudstone to sandstone interbeds; epidotized; volcanolithic conglomerate and sandstone.|
11844|Miller Basalt|72443|6|Mentioned|p738-739|||Talbot Sub-basin.||Cassidy Group||||
11849|Millidie Creek Formation|7161|5|Briefly described|p96|||At least 1500m thick.||||Underlain by the Robinson Range Formation.|Comprises shallowing-upwards packages of laminated iron-formation, laminated chert, clastic ironstone, bedded carbonate and feldspatholithic wacke.|02-MAY-12
11849|Millidie Creek Formation|12099|5|Briefly described|p678 Fig.4, p682-3|Orosirian|Orosirian|||Unit in Padbury Group.||Overlies Robinson Range Formation.||04-MAR-13
11849|Millidie Creek Formation|22493|5|Briefly described|p96 Fig.6|||||||||
11849|Millidie Creek Formation|22694|5|Briefly described|p7|||||||||
11849|Millidie Creek Formation|22940|4|Described|Fig.6 p14|Paleoproterozoic|Paleoproterozoic|See also Table 2 p12. of Padbury Group.||||||07-NOV-08
11849|Millidie Creek Formation|23592|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Variation of Published name/misspelt. Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
11849|Millidie Creek Formation|23744|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
11849|Millidie Creek Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin||||||
11849|Millidie Creek Formation|23749|4|Described|p13|Proterozoic|Proterozoic|See also page 3 table 1. Of Padbury Group. Geological Province: Padbury Basin.||||||
11849|Millidie Creek Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||
11849|Millidie Creek Formation|23890|5|Briefly described|p21 Fig.11|||Of Padbury Group. Geological Province: Padbury Basin.||||||
11849|Millidie Creek Formation|29663|2|Defined|p53|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11849|Millidie Creek Formation|30010|4|Described|p45|||||||||
11849|Millidie Creek Formation|36551|6|Mentioned|Table 29|||||||||
11849|Millidie Creek Formation|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11849|Millidie Creek Formation|37213|5|Briefly described|p20|||||||||
11849|Millidie Creek Formation|37460|4|Described|p144|||||||||
11849|Millidie Creek Formation|38978|6|Mentioned|p165|||||||||
11849|Millidie Creek Formation|40938|6|Mentioned|p69|||||||||
11849|Millidie Creek Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
11849|Millidie Creek Formation|44927|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
11849|Millidie Creek Formation|49896|5|Briefly described|p2 Tb. 1|||Of Barnett (1975). Superseded by Millidie Formation.||||||
11849|Millidie Creek Formation|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Padbury Group.  Overlies Wilthorpe Formation.  Geological Province: Padbury Basin.||||||07-NOV-08
11849|Millidie Creek Formation|62289|5|Briefly described|plate 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Padbury Group; sandstone and shale; minor granular iron-formation; Geol. Prov: Padbury Basin.||||||
11849|Millidie Creek Formation|63866|5|Briefly described|p164|||Western Glengarry Basin.||Padbury Group||||
11849|Millidie Creek Formation|64580|4|Described|map legend||Paleoproterozoic|Of Padbury Group. Banded iron-formation; minor ferruginous sandstone and shale; Bedded dolomite and dolomitic siltstone.||||||09-DEC-08
11849|Millidie Creek Formation|65411|5|Briefly described|p88, p90.|Paleoproterozoic|Paleoproterozoic|||Topmost unit in Padbury Group.||Conformably overlies Robinson Range Formation.|Lithic wacke, dolomitic siltstone, iron-rich shale and siltstone, banded manganiferous iron-formation, chloritic siltstone.|
11849|Millidie Creek Formation|65419|5|Briefly described|p37, p45.|Paleoproterozoic|Paleoproterozoic|Of Barnett (1975) and Gee (1979); now includes a unit of laminated chlorite-quartz siltstone mapped by Occhipinti et al. (1996) within the Millidie syncline.||Unit in Padbury Group.||||
11849|Millidie Creek Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in upper Padbury Group. Quartz-chlorite-muscovite-(tourmaline-hematite) schist; muscovite-quartz schist with porphyroblasts of pyrite; iron-rich shale.||||||
11849|Millidie Creek Formation|66299|6|Mentioned|p208.|||Metasedimentary rocks deformed by Capricorn Orogeny.||||||
11849|Millidie Creek Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Padbury Group|||Banded iron-formation; minor ferruginous sandstone and shale; Bedded dolomite and dolomitic siltstone; Sandstone and shale; minor granular iron-formation.|
11849|Millidie Creek Formation|69003|5|Briefly described|p16|||Padbury Basin.||Padbury Group.||Conformably overlies Robinson Range Formation.|Ferruginous shales and siltstones.|
11849|Millidie Creek Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Padbury Basin.||Of the Padbury Group.||Overlies Wilthorpe Formation.|Sandstone and shale; minor granular iron-formation.|06-MAY-14
11849|Millidie Creek Formation|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Padbury Group|||Banded iron formation, bedded dolomite, dolomitic siltstone, sandstone and shale; minor ferruginous sandstone, shale and granular iron formation.|
11849|Millidie Creek Formation|69596|5|Briefly described|p10-11|||Padbury Basin. Shallow-water (lacustrine or marine platform) deposits.|||||Shales.|
11849|Millidie Creek Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1983-1811 Ma||||Sandstone and shale; minor granular iron formation|
11849|Millidie Creek Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Padbury Basin, Capricorn Orogen.|ca 19831811 Ma (inferred)|Padbury Group|||Sandstone and shale; minor granular ironformation.|
11849|Millidie Creek Formation|70804|5|Briefly described|p2-p3, p18, p20, p24, p26, plate 1|Early Proterozoic|Early Proterozoic|Defined by Barnett (1975) and modified by Gee (1979) and Occhipinti et al. (1997). Hosts numerous manganese deposits.||Padbury Group||Conformably overlies the Robinson Range Formation. Unconformably overlain by the Bangemall Group.|Sericitic siltstone, chloritic siltstone, banded iron-formation, dolomitic arenite.|
11849|Millidie Creek Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||siltstone, schist, banded iron formation, shale, crystalline carbonate, sandstone, phyllite, pelite|
11849|Millidie Creek 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.|1983-1811 Ma (inferred)|Unit of Padbury Group.|||Ferruginous shale and siltstone, schist, with porphyroblasts of pyrite; granular iron formation; bedded dolomite and dolomitic siltstone|
11849|Millidie Creek Formation|71484|4|Described|p124,125,130,134,137-138|Orosirian|Orosirian|Geological province: Of Padbury Basin. Deposited during continuous basin development in the western part of the basin, prior to c. 1820 Ma Capricorn Orogeny. Metamorphosed and deformed carbonate sedimentary rocks previously mapped as Millidie Creek Formation, which outcrop between the northern margin of the Yilgarn Craton and Yarlarweelor Gneiss Complex were reassigned to Juderina Formation based on continuity on potential field datasets and similar stratigraphic levels.||Unit of Padbury Group.||Overlain by Mooranie Supersuite. Underlain by Robinson Range Formation.|Banded iron formation, ferriginous to dolomitic sandstone, shale, siltstone, locally with granular iron formation.|30-AUG-19
11849|Millidie Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Padbury Basin.||Padbury Group|||Sandstone and shale; minor granular iron-formation.|
11862|Milligans Formation|5256|5|Briefly described|p143, p144, p148.|Visean|Tournaisian|Bonaparte Basin. Type section: Milligans 1 (44-155m). Rare conodonts indicate age ~ Tournaisian - Visean boundary, but elsewhere stated as latest Tournaisian - late Visean. Widespread clastic marine unit. Wave protected, calm, shallow water environment||||||
11862|Milligans Formation|7142|6|Mentioned|p350 Fig.4.|Early Carboniferous|Early Carboniferous|Browse Basin.||||Overlies Bonaparte Formation. Is overlain by Tanmurra Formation.||
11862|Milligans Formation|13194|6|Mentioned|p390 Tb. 4-16; p382, 402 figs 4-59,-66|Visean|Tournaisian|Type Section: Milligans 1 well (44-155m); Reference section: Bonaparte 1 well (497-2280m).  300 to 2142m thick offshore marine deposits.||Weaber Group||Unconformably overlies Bonaparte Formation; Cockatoo, Ningbing and Langfield Groups; overlies Bonaparte Formation (conformably). Conformably underlies Utting Calcarenite and Waggon Creek Formation.|Shale; minor siltstone and sandstone.|
11862|Milligans Formation|13234|5|Briefly described|p248, p250-256, p260,262 Tbs.1,2; p265.|Early Carboniferous|Early Carboniferous|Source rock for oil at Turtle and Barnett reservoirs. Deposited during rapid deepening. Proven regional top seal.|||||Marine anoxic shales.|
11862|Milligans Formation|13354|6|Mentioned|p375 Fig.6.|Early Carboniferous|Early Carboniferous|Overlies Bonaparte Formation and underlies Tanmurra Formation.||62||||28-OCT-14
11862|Milligans Formation|14228|5|Briefly described|p6 fig3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||Overlain by Tanmurra Formation.||05-OCT-16
11862|Milligans Formation|22663|5|Briefly described|W97 8 to 10 p2 Fig.3||Carboniferous|||||||01-MAR-10
11862|Milligans Formation|23356|5|Briefly described|26 Tab.2|Early Carboniferous|Early Carboniferous|||||||
11862|Milligans Formation|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||06-NOV-06
11862|Milligans Formation|24246|5|Briefly described|p7|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24378|5|Briefly described|p14|||Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|24569|5|Briefly described|p248 Fig. 3|Visean|Visean|Of the Weaber Group.Geological Province: Petrel Sub-basin.||||||02-MAR-05
11862|Milligans Formation|40792|5|Briefly described|p175|||Mention Fig.3.||||||06-NOV-06
11862|Milligans Formation|40993|6|Mentioned|p9|||Mention Fig.1||||||
11862|Milligans Formation|41459|6|Mentioned|p278|||||||||
11862|Milligans Formation|41532|5|Briefly described|p292|||||||||
11862|Milligans Formation|41690|6|Mentioned|p57|||||||||
11862|Milligans Formation|41731|6|Mentioned|p574|||||||||
11862|Milligans Formation|41839|4|Described|p31|||Formerly "Milligans Beds"||||||
11862|Milligans Formation|41864|3|Fully described|p123|||||||||
11862|Milligans Formation|41865|5|Briefly described|Map legend|late Visean|late Tournaisian|||||||
11862|Milligans Formation|41867|5|Briefly described|Map legend|late Visean|late Tournaisian|||||||
11862|Milligans Formation|42030|5|Briefly described|p750|||||||||
11862|Milligans Formation|42055|4|Described|Fig.1 P52|||||||||
11862|Milligans Formation|42056|6|Mentioned|p96|||||||||
11862|Milligans Formation|42175|5|Briefly described|p197|||||||||
11862|Milligans Formation|42442|3|Fully described|p11|Visean|Tournaisian|NT. Age latest Tournaisian to late Visean.||||||
11862|Milligans Formation|42547|4|Described|p101|||||||||
11862|Milligans Formation|43482|6|Mentioned|23||Early Carboniferous|||||||
11862|Milligans Formation|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
11862|Milligans Formation|49637|5|Briefly described|Fig. 6|Early Carboniferous|Early Carboniferous|Age: ~350Ma. Geological Province: Bonaparte Basin.||||||07-FEB-11
11862|Milligans Formation|50085|5|Briefly described|p2 Fig. 2, p3 Tb.1|Carboniferous||Shaly unit.  Geological Province: Bonaparte Basin.||||||11-MAY-04
11862|Milligans Formation|60006|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Bonaparte Basin. Of the Weaber Group. Shale, siltstone, minor sandstone.||||||22-JUL-04
11862|Milligans Formation|60364|4|Described|p184, 189, 196|Visean|Tournaisian|Overlies Langfield Group and Bonaparte Formation (unconformable). Conformably overlain by Utting Calcarenite and Burvill Formation. Max. thickness: 2143m. Offshore shales and other marine clastics. Fossiliferous. Geological Province: Bonaparte Basin.||||||11-MAY-05
11862|Milligans Formation|60682|4|Described|p22 Table 5, 24|Visean|Tournaisian|Of Weabar Group. Unconformably overlies Langfield Group. Thickness: 2142m. Shale and siltstone, minor sandstone. Prograding delta and alluvial fan. Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|60701|5|Briefly described|p13|Early Carboniferous|Early Carboniferous|Contains oil in its marine shales.  Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||11-APR-08
11862|Milligans Formation|61250|6|Mentioned|p45|Carboniferous|Carboniferous|Unconformably overlies the Langford Group.  Geological Province: Bonaparte Basin.||||||
11862|Milligans Formation|61542|1|Redefined|p276, p277 Fig. 2|Visean|Tournaisian|Of Beere(1984). Gorter et al(2005) subdivided off part as Yow Fm.and relegated Waggon Creek Fm. to W.C. facies.Of Weaber Gp (basal) - fossiliferous shales and siltstone. Unconformable on Bonaparte Fm. Geol.province: onshore Bonapart Basin/Petrel-Sub-basin.||||||17-JUN-13
11862|Milligans Formation|62759|5|Briefly described|p1|Carboniferous|Carboniferous|Stated to unconformably overlie Langford Group - which should be Langfield Group.||||||
11862|Milligans Formation|62837|5|Briefly described|Stratigraphic columns|Visean|Tournaisian|Of the Weaber Group.  Age: <345-~328Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
11862|Milligans Formation|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
11862|Milligans Formation|64689|5|Briefly described|p16, p20 |Carboniferous|Carboniferous|Previously, thought to be the source of oil discoveries at Turtle-1 and Barnett-1; Gorter et al. (2004) suggest otherwise (the Langfield Group).||Basal unit in Weaber Group.||Overlies the Langfield Group unconformably.||
11862|Milligans Formation|64694|5|Briefly described|p231-241, p242 Tb.4, p243-244|Visean|Late Tournaisian|See also p245 Fig.9, p246-249, p252. Divided into a lower and an upper part by Lee and Gunn (1988). Previous to this study, marine shales in this unit were regarded as the source of Early Carboniferous to Permian-reservoired oils in the offshore Turtle and Barnett wells. The authors say that there is no compelling evidence that this unit contains oil-prone source beds where it has been sampled.||Unit in Weaber Group.||Unconformably overlies Bonaparte Formation and Langfield Group. Is overlain unconformably by Tanmurra Formation.||
11862|Milligans Formation|65331|5|Briefly described|Map legend|Visean|Visean|Of Bonaparte Basin. Of Weaber Group. Shale, siltstone, minor sandstone||||||
11862|Milligans Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes heterolithic fine-grained light grey sandstone and dark grey siltstone; slumping features; whispy siltstone in the sandstone.|
11862|Milligans Formation|67200|5|Briefly described|app 2 p8||||||||Heterolithic fine grained sandstone and siltstone; slumping features.|
11862|Milligans Formation|69099|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||03-AUG-15
11862|Milligans Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
11862|Milligans Formation|69452|4|Described|p36:9, 11-16, 24-25, 28|Early Carboniferous|Early Carboniferous|Caye (1968); Gorter et al. (2005). Petrel Sub-basin, Bonaparte Basin. Moderately deep marine deposits. Up to 2143m thick. Offshore and onshore. Incorporates the former Waggon Creek Formation, now as a facies association. An upper interval, above a major sequence boundary, was assigned to the Yow Creek Formation by Gorter et al. (2005). Latest Tournaisian to early Visean. Significant gas flows obtained in Keep River-1 and Weaber-1, -2A. Acted as a seal to the mineralising brine which produced the Sandy Creek Zn-Pb-Ag deposit. Also appears as Milligans Shale in Fig.32.19. Has produced dry gas flows in most cases where it is intersected.||Weaber Group.||Unconformably overlies Septimus Limestone (Langfield Group) and (locally) Buttons Formation. Is overlain unconformably by Utting Calcarenite and Yow Creek Formation.|A recessive unit. Offshore: mostly fossiliferous silty shale. Onshore intersections also include interbedded sandstone, limestone (packstone and grainstone), and conglomerate of the Waggon Creek facies association. Abundant fauna and microflora.|12-JUL-16
11862|Milligans Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
11862|Milligans Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Bonaparte Formation. Is overlain by Yow Creek Formation.||
11862|Milligans Formation|69673|5|Briefly described|p168 fig 138, p171, p178, p181, p184|Early Carboniferous||Proven gas reservoir.||Weaber Group||Overlies Langfield Group, Buttons Formation, overlain by Yow Creek Formation|Fossiliferous silty shale and interbedded sandstone, limestone and conglomerates.|
11862|Milligans Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2-3|Visean|Tournaisian|See also Regional geology: Fig.8, p8-9, p11-13, p16. Sandstones and shales filling in an incised channel system in the Bonaparte Formation. Hydrocarbon source and reservoir rocks and a regional seal. Oil- and gas-prone mudstones, previously attributed to this unit, are assigned to a Langfield Group equivalent. Hosts conventional and unconventional gas resources in the Weaber gas field and elsewhere.||Weaber Group.||Overlies Bonaparte Formation and Langfield Group. Is overlain by Yow Creek Formation.||12-JUL-16
11862|Milligans Formation|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Weaber Group|||Shale, siltstone, minor sandstone.|
11862|Milligans Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Weaber Group.|||Black and dark grey shale, partly calcareous; minor limestone; rare fine to medium-grained sandstone; thin to thick beds; diverse fauna|
11862|Milligans Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Overlain by Yow Creek Formation.||
11877|Milyering Member|23726|5|Briefly described|p93 Fig 29|||Overlying unit Muiron Member. Underlying unit Jurabi Member.||||||04-DEC-06
11877|Milyering Member|33593|2|Defined|p114|Pleistocene|Pleistocene|Prob. Pleistocene. Type locality described.||||Muiron  Member disconformably underlies.||16-APR-18
11877|Milyering Member|37016|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
11877|Milyering Member|39427|4|Described|Table 1|||||||||
11877|Milyering Member|41271|4|Described|p194|||||||||
11877|Milyering Member|42116|5|Briefly described|p71|||||||||
11877|Milyering Member|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore. Occupies a terrace between Jurabi and Milyering Scarps.||Exmouth Sandstone.||Overlies Pilgramunna Formation.|Coarse-grained littoral deposits overlain by medium-grained aeolian deposits.|
11883|Minchin Siltstone|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
11883|Minchin Siltstone|32165|6|Mentioned|p195|||Refers Edgell (1964)||||||
11883|Minchin Siltstone|33022|6|Mentioned|p259|||||||||
11883|Minchin Siltstone|34008|6|Mentioned|p73|||Triassic||||||
11883|Minchin Siltstone|34287|6|Mentioned|p151|||||||||
11883|Minchin Siltstone|41271|6|Mentioned|p119|||||||||
11883|Minchin Siltstone|61811|5|Briefly described|p21, p64.|||Of Johnson and Playford (1958); thought to be Lower Jurassic, this unit was abandoned in favour of Kockatea Shale after Edgell (1964a) described Owenitian (=Olenekian) ammonoid impressions. Its type section was on Sugarloaf Hill; further details in Appendix 1. Typo 'Michin Siltstone' on p64.||||||
11908|Mingenew Formation|14227|5|Briefly described|Enclos. 2|Artinskian|Artinskian|Presented as Mingenew only - Formation inferred.||||||07-FEB-11
11908|Mingenew Formation|23172|4|Described|Map Legend|Permian|Permian|||||||
11908|Mingenew Formation|23279|5|Briefly described|p16|||Former Name: Mingenew Beds (Maitland, 1919).||||||
11908|Mingenew Formation|23816|4|Described|p235, 236|Artinskian|Artinskian|Formerly known as the "Mingenew Beds". Geologcial Province: Perth Basin. Max. thickness: 91 m. Equivalent to the Carynginia Formation.||||||16-DEC-04
11908|Mingenew Formation|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
11908|Mingenew Formation|30545|6|Mentioned|Fig.2|||Artinskian||||||
11908|Mingenew Formation|30963|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
11908|Mingenew Formation|31910|3|Fully described|Table 1|||P18||||||
11908|Mingenew Formation|32648|6|Mentioned|p32|||L. Perm.||||||
11908|Mingenew Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
11908|Mingenew Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
11908|Mingenew Formation|34532|6|Mentioned|p226|||Fig.2||||||
11908|Mingenew Formation|36208|6|Mentioned|p253|||||||||
11908|Mingenew Formation|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
11908|Mingenew Formation|36293|2|Defined|p115|Permian|Permian|||||||
11908|Mingenew Formation|36890|3|Fully described|p235|||Formerly Mingenew Beds.||||||
11908|Mingenew Formation|37104|6|Mentioned|Fig.3|||||||||
11908|Mingenew Formation|37286|6|Mentioned|p30|||||||||
11908|Mingenew Formation|37298|6|Mentioned|Fig.1|||||||||
11908|Mingenew Formation|37549|6|Mentioned|p119|||||||||
11908|Mingenew Formation|41049|6|Mentioned|p43|||||||||
11908|Mingenew Formation|41071|6|Mentioned|p27|||||||||
11908|Mingenew Formation|41315|6|Mentioned|p155|||||||||
11908|Mingenew Formation|42462|6|Mentioned|p62|||Perth Basin||||||
11908|Mingenew Formation|42994|6|Mentioned|p70|||||||||
11908|Mingenew Formation|43015|5|Briefly described|Table 1,p319|||||||||
11908|Mingenew Formation|43296|5|Briefly described|Map Legend||Permian|||||||
11908|Mingenew Formation|43495|4|Described|6-26||Artinskian|||||||
11908|Mingenew Formation|44144|4|Described|p508 Tb.4-21, p510-511, p513|Artinskian|Artinskian|Type Section: Simpson Knolls; 29o11'50''S 115o28'02''E. 90m thick shallow marine sediments containing plant remains, brachiopods and molluscs.|||||Red-brown to yellow, very fine- to medium-grained sandstone and micaceous siltstone.|
11908|Mingenew Formation|44219|14|Not recorded|p31||Artinskian|||||||
11908|Mingenew Formation|44237|14|Not recorded|p.197,201,203||Permian|(L.Permian).||||||
11908|Mingenew Formation|44994|6|Mentioned|Fig.7|||Permian. Correlation.||||||
11908|Mingenew Formation|45001|14|Not recorded|p146|||||||||
11908|Mingenew Formation|48857|14|Not recorded|p.15|||||||||
11908|Mingenew Formation|49644|5|Briefly described|Table|||||||||
11908|Mingenew Formation|61811|5|Briefly described|p36, p64.|Permian|Permian|Lateral equivalent of the lower part of the Carynginia Formation. Type section details in Appendix 1.|||||Fossiliferous marine deposits.|
11908|Mingenew Formation|64580|4|Described|map legend||Early Permian|Fine- to medium-grained sandstone, micaceous siltstone.||||||09-DEC-08
11908|Mingenew Formation|64635|5|Briefly described|p18 |||Fossiliferous marine facies.||||Appears to be laterally equivalent to the lower part of the Carynginia Formation.||
11908|Mingenew Formation|64974|6|Mentioned|p145|Artinskian|Artinskian|Geological Province: Perth Basin.||||||24-JUN-09
11908|Mingenew Formation|69182|6|Mentioned|Ch2 p3|||Perth Basin.||||||
11908|Mingenew Formation|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)||||Fine to mediumgrained sandstone, micaceous siltstone|
11908|Mingenew Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone, conglomerate, sandstone|
11908|Mingenew Formation|71269|5|Briefly described|500k_interpgeop16_lut.csv|Kungurian|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);??|286-272.3 Ma (biostrat)||||Fine- to coarse-grained sandstone, micaceous siltstone|
11908|Mingenew Formation|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Artinskian|Perth Basin.  Age from biostratigraphy.||Permian package 2, Perth Basin.|||Fine- to coarse-grained sandstone, micaceous siltstone.|
11914|Minim Cove Member|22552|6|Mentioned|p 41|||||||||
11914|Minim Cove Member|41245|6|Mentioned|p33|||||||||
11914|Minim Cove Member|41831|4|Described|p557|||||||||
11914|Minim Cove Member|62369|6|Mentioned|p414|||Of Tamala Limestone. Geological Province: Perth Basin.||||||
11914|Minim Cove Member|69788|6|Mentioned|p1035|||Marine unit in Swan River estuary; deposited during Marine Isotope Stage 5.||||Coeval with Grey Member.||
11957|Miria Formation|12491|6|Mentioned|p454 Fig.7.|||Presented in figure as Cardabia and Miria Formations.||||||06-NOV-14
11957|Miria Formation|12729|5|Briefly described|p. 17||Cretaceous|Type section along Toothawarra Creek in the Giralia Anticline (Hocking et al., 1987). Only penetrated by Airey Hill 1  in Gascoyne Platform (just south of Cardabia Transfer Fault) - either not deposited or eroded over rest of platform. Deposited in a low-medium energy, marine-shelf environment.||||Disconformably overlies the Korojon Calcarenite.|Calcarenite and calcisiltite.|
11957|Miria Formation|14228|5|Briefly described|p9, p16|Late Cretaceous|Late Cretaceous|Thickness from 0.6 m to 95 m.||||Overlies (disconformably) Korojon Calcarenite or Toolonga Calcilutite.|Calcarenite and calcisiltite deposited in a low- to medium-energy, marine shelf environment.|
11957|Miria Formation|23183|6|Mentioned|p217-8|Maastrichtian||||||||
11957|Miria Formation|23188|6|Mentioned|p287||Maastrichtian|||||||
11957|Miria Formation|23403|4|Described|p9|Cretaceous|Cretaceous|Formerly Miria Marl.||||||24-NOV-09
11957|Miria Formation|23572|5|Briefly described|p12|Late Cretaceous|Late Cretaceous|Geological Province: Carnarvon Basin. Underlying Unit: Toolonga Calcilutite.||||||
11957|Miria Formation|23620|5|Briefly described|p4 Fig. 4|Cretaceous|Cretaceous|Predominantly calcareous pelagic deposits||||||
11957|Miria Formation|23726|5|Briefly described|p7 Fig 2b|Late Cretaceous|Late Cretaceous|Underlying unit Toloonga Calcilutite. Geological Province: Carnarvon Basin.||||||
11957|Miria Formation|23915|5|Briefly described|p518 Table 1|Late Cretaceous|Late Cretaceous|Geological Province: Southern Carnarvon Basin.||||||
11957|Miria Formation|23976|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
11957|Miria Formation|23977|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
11957|Miria Formation|23978|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
11957|Miria Formation|24094|4|Described|p268, p275|Maastrichtian|Maastrichtian|Overlies disconformably the Korojon Calcarenite. Overlain disconformably by the Boongerooda Greensand. Maximum thickness: 2.1m. Geological Province: Carnarvon Basin||||||16-MAR-05
11957|Miria Formation|40144|4|Described|p306|||||||||
11957|Miria Formation|40617|5|Briefly described|p15|||Mention P18||||||
11957|Miria Formation|40992|6|Mentioned|Fig.8|||||||||
11957|Miria Formation|41112|5|Briefly described|p419|||||||||
11957|Miria Formation|41271|3|Fully described|p160|||||||||
11957|Miria Formation|41422|6|Mentioned|p163|||||||||
11957|Miria Formation|41438|6|Mentioned|p109|||||||||
11957|Miria Formation|41440|4|Described|p139|||||||||
11957|Miria Formation|41446|6|Mentioned|p203|||||||||
11957|Miria Formation|41732|6|Mentioned|Fig.3|||||||||
11957|Miria Formation|42116|5|Briefly described|Fig.1 P6|||||||||
11957|Miria Formation|42123|5|Briefly described|p37|||See also Fig.13||||||
11957|Miria Formation|42374|4|Described|p436-437|Maastrichtian||Supersedes Miria Marl?||||||
11957|Miria Formation|42473|6|Mentioned|p14|||||||||
11957|Miria Formation|42477|5|Briefly described|p156|||||||||
11957|Miria Formation|42563|4|Described|p133, 166|||||||||
11957|Miria Formation|43173|5|Briefly described|13||Late Cretaceous|||||||
11957|Miria Formation|43564|6|Mentioned|Fig.2,p446||Maastrichtian|||||||
11957|Miria Formation|44143|4|Described|p430 Table 4-19; p449 Figure 4-108, p450|Cretaceous|Cretaceous|>400m thick; shale and limestone; marine. Conformably overlies Toolonga Calcilutite. Bedout Sub-basin.||||||23-NOV-17
11957|Miria Formation|60384|5|Briefly described|p244||Late Cretaceous|Southern Carnarvon Basin. Latest Cretaceous. See also Miria Marl Fig. 2.|||||Low-energy marine-shelf calcarenite and calcisiltite.|
11957|Miria Formation|61155|5|Briefly described|p15|||Age is pre-Cainozoic. Geological Province: Carnarvon Basin (Exmouth Plateau, onshore and offshore).||||||
11957|Miria Formation|62734|5|Briefly described|p1362 Fig. 2|Paleocene|Late Cretaceous|Geological Province: Barrow Sub-basin. See also p1375.||||||01-SEP-08
11957|Miria Formation|67200|5|Briefly described|p8 fig 6, p53|Cretaceous|Cretaceous|Thermal conductivity of 1.68 W/mK||||Unconformably overlies Toolonga Calcilutite|Crudely bedded marl.|
11957|Miria Formation|67368|6|Mentioned|p209 Fig.4.|Maastrichtian|Maastrichtian|||||||
11957|Miria Formation|67970|6|Mentioned|p25 Fig.4.|Maastrichtian|Maastrichtian|Exmouth Plateau.||||||
11957|Miria Formation|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|||Carnarvon Basin. See also  Ch3  p23, Ch3 p35, Ch3 p37, Ch3 p65-p66, Ch3 p73.||||Disconformably overlain by the Cardabia Calcarenite. Overlies the Toolonga Calcilutite.||
11957|Miria Formation|69297|6|Mentioned|p249, p337|Maastrichtian|Maastrichtian|Gascoyne Sub-basin of the Southern Carnarvon Basin and the Canning, Roebuck Basins.||||Unconformably overlies the Korojon Calcarenite. Overlies the Toolonga Calcilutite.  Unconformably overlain by the Cardabia and Giralia Calcarenites.||
11957|Miria Formation|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Maastrichtian|Maastrichtian|Roebuck Basin and offshore Canning Basin.||||Overlies Toolonga Calcilutite.||
11957|Miria Formation|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Maastrichtian|Maastrichtian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Withnell Formation. Is overlain by Lambert Formation.||
11957|Miria Formation|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Plateau.||||Overlies Korojon Calcarenite.||
11971|Mission Group|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Central Officer Basin||||||
11971|Mission Group|24161|5|Briefly described|p6|||Overlain by the Townsend Quartzite.||||||25-JUL-06
11971|Mission Group|30388|4|Described|Table 1|||Middle Proterozoic age||||||
11971|Mission Group|30390|4|Described|p77|||See also p78-81||||||25-JUL-06
11971|Mission Group|30391|5|Briefly described|p456|||||||||
11971|Mission Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
11971|Mission Group|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11971|Mission Group|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11971|Mission Group|31914|6|Mentioned|p95|||||||||
11971|Mission Group|36551|6|Mentioned|Table 31|||||||||
11971|Mission Group|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
11971|Mission Group|36886|4|Described|p197|||||||||
11971|Mission Group|37707|6|Mentioned|p24|||||||||
11971|Mission Group|38243|6|Mentioned|p355|||See also Fig.2.||||||
11971|Mission Group|44109|6|Mentioned|p163|||Of the Bentley Supergroup? Sedimentary rocks.||||||
11971|Mission Group|44139|5|Briefly described|p284, Table 3-16, p286|||Of Bentley Supergroup. 4500m. Basalt, dolomite, conglomerate. Overlain by Townsend Quartzite.|| ||||10-SEP-12
11971|Mission Group|45149|5|Briefly described|p19|||||||||
11971|Mission Group|50205|6|Mentioned|p60 |||Could be related to the basin concealed by the Officer Basin.||||||
11971|Mission Group|62453|6|Mentioned|p15|||Of the Bentley Supergroup.||||||
11971|Mission Group|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
11971|Mission Group|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup. Conglomerate, sandstone, shale, and basalt; minor tuff, dolomite, and quartzite.||||||09-DEC-08
11971|Mission Group|65102|6|Mentioned|p363, Fig. 4-38, p364|Mesoproterozoic|Mesoproterozoic|Paterson Orogen (SE). Of Bentley Supergroup. Underlies Officer Basin.||||||
11971|Mission Group|65410|6|Mentioned|p73 Fig.2.|Proterozoic|Proterozoic|Western Officer Basin.||||||
11971|Mission Group|65416|6|Mentioned|p137 Fig.2.|Mesoproterozoic|Mesoproterozoic|Western Officer Basin.||||||
11971|Mission Group|67375|5|Briefly described|p7, p16 Fig.10, p38 table 1, pp49-53.|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Musgrave Region. Total thickness of 4,000 m.||Topmost unit in Bentley Supergroup.|Includes Gamminah Conglomerate; Frank Scott, Lilian and Milesia Formations.|Conformably overlies Cassidy Group. Is conformably overlain by Townsend Quartzite.|Conglomerates and sandy siliciclastics in the lower part.|
11971|Mission Group|67553|5|Briefly described|p8,17,40-42,53,59,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Total thickness: 4000m.||Unit of Bentley Supergroup.|Includes Milesia Formation, Lilian Formation, Frank Scott Formation and Gamminah Conglomerate.|Overlain by Townsend Quartzite. Underlain by Cassidy Group/Miller Basalt.||
11971|Mission Group|68995|4|Described|p3 Fig.1, p4 Fig.2, p7 Fig.3, p9-10 |Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. Estimated 4000m thick. See also p19, p49 Fig.25.|c. 1085-1040 Ma|Bentley Supergroup|Gamminah Conglomerate, Frank Scott Formation, Lilian Formation, Milesia Formation|Conformably overlies the Cassidy Group. Conformably to unconformably overlain by the Townsend Quartzite.|Conglomerate, sandy siliciclastic and calcareous rocks.|
11971|Mission Group|68996|5|Briefly described|p5, p7, p32, p36, p47, p50, 65|Mesoproterozoic|Mesoproterozoic|Age of Cassidy and Mission Groups given as 1065-1050 Ma. Essentially undeformed.||Bentley Supergroup|||Mainly intercalated basalt and rhyolites.|
11971|Mission Group|69003|4|Described|p37, p51-52|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province. Up to 4000m thick.|< 1057 Ma.|Topmost unit in the Bentley Supergroup.||Conformably overlies Cassidy Group. Is overlain unconformably by Bitter Springs Formation.|Lower part dominated by conglomerates, sandstones and shales; upper part mainly basalt.|
11971|Mission Group|69091|4|Described|p30 Fig.3.5, p41 Fig.3.8, see comments|||Talbot Sub-basin, Musgrave Province. Youngest preserved stratigraphic interval of Bentley Supergroup. Total thickness: about 4000m (Daniels, 1974). See also p44, p52 Fig.4.1, p54 Fig.4.2, p59 Fig.4.6, p71 Fig.4.14, p75, p81 Fig.4.17, p84, p106 Fig.5.7a, p107 Fig.5.8a, p108 Fig.5.9, p109 Fig.5.10, p114, p115 Fig.5.14, p117 Fig.5.15, p119 Fig.5.16, p131 Fig.6.1, p133, p134 Fig.6.2, p144-145, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||Bentley Supergroup||Conformably overlies Cassidy Group; is overlain by Townsend Quartzite.|Sedimentary lower part, and upper basalt dominated part.|
11971|Mission Group|69153|5|Briefly described|geologyp_lut.csv 500k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Milesia Formation, Lilian Formation, Frank Scott Formation, Gamminah Conglomerate||Vesicular and amygdaloidal basalt and basaltic andesite, interlayered with fine- to coarse-grained siliciclastic rocks and minor dolomite, chert, and microbialite|
11971|Mission Group|69655|5|Briefly described|p3, p6|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||||
11971|Mission Group|69729|5|Briefly described|p66 Fig.1, p70, p80, p82|||The youngest stratigraphic interval of the Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.||Conformably overlies the Cassidy Group.|A sedimentary lower part is overlain by an upper basalt-dominated part.|
11971|Mission Group|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin.||Unit of Bentley Supergroup.||Uppermost unit of Bentley Supergroup. Overlain by Buldya Group. Underlain by Cassidy Group/Miller Basalt.||
11971|Mission Group|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Gamminah Conglomerate; Frank Scott, Lilian, Milesia Formations.||Conglomerate, sandstone, shale, limestone, basalt and basaltic andesite.|12-NOV-15
11971|Mission Group|70634|4|Described|500k_geologyp08_lut,csv|Mesoproterozoic|Mesoproterozoic|||Bentley Supergroup|Includes Frank Scott Formation, Gamminah Conglomerate, Lilian Formation, Milesia Formation||Conglomerate, sandstone, shale, and basalt; minor tuff, dolomite, and quartzite.|
11971|Mission Group|70793|5|Briefly 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.|1057-1040 Ma (inferred)|Unit of Bentley Supergroup.|Includes Frank Scott Formation, Gamminah Conglomerate, Lilian Formation, Milesia Formation.|||
11971|Mission Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup||||
11971|Mission Group|70831|5|Briefly described|p3, p5|||Musgrave Province.||Bentley Supergroup||||
11971|Mission Group|71170|5|Briefly described|p5|||Talbot Sub-basin. Emplaced during the Giles Event.||||||
11971|Mission Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
11971|Mission Group|71211|5|Briefly described|p6 fig 1.3, p7 fig 1.4, p12|||See also p24 fig 2.1, p25, p26, p84 fig 3.1, p86, p136 fig 4.1, p216, p234.||Bentley Supergroup||Overlies the Pussy Cat Group. Conformably overlies the Cassidy Group.  Conformably or unconformably overlain by the Townsend Quartzite.|Basalts and sedimentary rocks.|
11971|Mission Group|71268|5|Briefly 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, 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.||Unit of Bentley Supergroup.|Includes Frank Scott Formation, Gamminah Conglomerate, Lilian Formation, Milesia Formation.|||
11971|Mission Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|||Vesicular and amygdaloidal basalt and basaltic andesite, interlayered with fine- to coarse-grained siliciclastic rocks and minor dolomite, chert, and microbialite.|
11971|Mission Group|72094|4|Described|p3 Fig 2, p4-5, 13|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Bentley Basin. Youngest unit of the Bentley Supergroup.||Unit of Bentley Supergroup.|||Vesicular and amygdaloidal basalt and basaltic andesite interlayered with fine- to coarse-grained siliciclastic rocks, minor dolostone, chert and possible microbialite.|
11971|Mission Group|72443|5|Briefly described|p737-740|||Talbot Sub-basin. Youngest unit of Talbot Sub-basin. Unconformably overlain by the Neoproterozoic units of the Officer Basin.||Bentley Supergroup||Conformably overlies the Cassidy Group.|Sedimentary lower part and a basalt-dominated upper part.|
11971|Mission Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
11996|Mittiwali Member|30565|6|Mentioned|p117|||||||||
11996|Mittiwali Member|32164|6|Mentioned|p488|||||||||
12027|Mokadine Formation|24160|6|Mentioned|p26, p27 Tb.14|Proterozoic|Proterozoic|||Basal unit in Coomberdale Subgroup.||||
12027|Mokadine Formation|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Basal unit of the Coomberdale Subgroup (Moora Group). Arkose with sandstone, siltstone, chert. See also p142 Tb. 60. p143 Fig. 83.||||||24-NOV-09
12027|Mokadine Formation|34705|6|Mentioned|p398|||||||||
12027|Mokadine Formation|36293|2|Defined|p64|Proterozoic|Proterozoic|||||||
12027|Mokadine Formation|36872|3|Fully described|p76|||||||||
12027|Mokadine Formation|37460|6|Mentioned|p178|||||||||
12027|Mokadine Formation|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12027|Mokadine Formation|40347|6|Mentioned|p16|||||||||
12027|Mokadine Formation|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
12027|Mokadine Formation|40349|5|Briefly described|p13|||||||||
12027|Mokadine Formation|42038|6|Mentioned|p108|||||||||
12086|Monday Hill Adamellite|40775|4|Described|p500|||||||||
12089|Mondooma Granite|23722|5|Briefly described|p9|Proterozoic|Proterozoic|Porphyritic micromonzonite. Geological Province: Hooper Complex||||||06-AUG-08
12089|Mondooma 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
12089|Mondooma Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12089|Mondooma Granite|30533|5|Briefly described|p13|||On Table 1||||||
12089|Mondooma Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12089|Mondooma Granite|30896|4|Described|p13|||Lower Proterozoic||||||
12089|Mondooma Granite|30897|5|Briefly described|p9|||||||||
12089|Mondooma Granite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12089|Mondooma Granite|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12089|Mondooma Granite|32728|6|Mentioned|Table 4|||||||||
12089|Mondooma Granite|36885|4|Described|p171|||||||||
12089|Mondooma Granite|37633|4|Described|Table 65|||See also p97.||||||08-MAY-15
12089|Mondooma Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
12089|Mondooma Granite|42811|5|Briefly described|p9|||||||||
12089|Mondooma Granite|42814|5|Briefly described|p7|||||||||
12089|Mondooma Granite|42815|5|Briefly described|map|||||||||
12089|Mondooma Granite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
12089|Mondooma Granite|44155|4|Described|p241 Tb.3-4|||||Hooper Complex||Intrudes Mount Disaster Porphyry.|Pale-grey porphyritic biotite granite and microgranite, and biotite-hornblende-orthopyroxene microgranodiorite; bipyramidal quartz and feldspar phenocrysts.|
12089|Mondooma Granite|48931|3|Fully described|p25|||||||||
12089|Mondooma Granite|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
12089|Mondooma Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1862 Ma|Paperbark Supersuite||||
12089|Mondooma Granite|68078|6|Mentioned|p14 figure 10|Paleoproterozoic|Paleoproterozoic|||Paperbark Supersuite|||Granite.|
12089|Mondooma Granite|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 this high-level granite.|1862+/-4 Ma U/Pb SHRIMP|Paperbark Supersuite|||Foliated biotite metamicromonzogranite with quartz phenocrysts; minor metasyenogranite and metagranodiorite.|03-AUG-15
12089|Mondooma Granite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Neoarchean||1862-2571 Ma|||||
12089|Mondooma Granite|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.|1862 Ma (isotopic)|Unit of Paperbark Supersuite.|||Foliated biotite metamicromonzogranite with quartz phenocrysts; minor metasyenogranite and metagranodiorite|
12089|Mondooma Granite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|c.1862 Ma; Griffin et al. (2000).|Unit in Paperbark Supersuite.|||Foliated biotite metamicromonzogranite with quartz phenocrysts; minor metasyenogranite and metagranodiorite.|
12089|Mondooma Granite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|c.1862 Ma (Griffin et al., 2000).|Paperbark Supersuite.|||Foliated biotite metamicromonzogranite with quartz phenocrysts; minor metasyenogranite and metagranodiorite.|
12089|Mondooma Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_geologyp_lut.csv|1862 Ma|Paperbark Supersuite|||Foliated biotite metamicromonzogranite with quartz phenocrysts; minor metasyenogranite and metagranodiorite.|
12089|Mondooma 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, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1862+\-4 Ma (isotopic)|Unit of Paperbark Supersuite.||Intruded by Lennard Granite.|Foliated quartz-phyric biotite micromonzogranite with minor syenogranite and granodiorite|
12089|Mondooma Granite|72437|5|Briefly described|p34-36|||Whole-rock analyses are provided.|||||Monzogranite.|
12101|Mongoloo Sandstone|40466|6|Mentioned|p68|||||||||
12126|Montara Formation|5952|5|Briefly described|p215 Fig. 5|||Appears as Montara in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
12126|Montara Formation|7142|6|Mentioned|p350 Fig.4.|Late Jurassic|Middle Jurassic|Browse Basin.||||Overlies Plover Formation. Is overlain by Lower Vulcan Formation.||
12126|Montara Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||07-NOV-06
12126|Montara Formation|23378|6|Mentioned|p180 Fig.2|Late Jurassic|Middle Jurassic|Of the Swan Group.  In the Vulcan Sub-basin.||||||07-NOV-06
12126|Montara Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
12126|Montara Formation|42053|4|Described|p40|||See also Fig.2||||||01-MAR-10
12126|Montara Formation|42395|5|Briefly described|p81|||||||||
12126|Montara Formation|43826|6|Mentioned|Fig.2,p163||Middle Jurassic|||||||01-MAR-10
12126|Montara Formation|61550|6|Mentioned|p495 Fig.2. |Callovian|Callovian|||Unit in Swan Group.||||
12126|Montara Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Jurassic|Age: ~163-~156Ma. Geological Province:  Vulcan Sub-basin.||||||01-MAR-10
12126|Montara Formation|63358|5|Briefly described|p4 Fig. 1.3|Oxfordian|Callovian|||||||01-MAR-10
12126|Montara Formation|64689|5|Briefly described|p7 Fig.6, p14-15|Late Jurassic|Middle Jurassic|See also references to mis-spelt Montara Sandstone (p8-9). A near top reservoir reflector.||||||
12126|Montara Formation|64696|6|Mentioned|p125, p127 Fig.2, p131, p134, p136-137|Late Jurassic|Middle Jurassic|Deposition in fan-deltas and alluvial fans.|||||Sandstones, shales.|
12126|Montara Formation|64697|6|Mentioned|p89 |Late Jurassic|Late Jurassic|In 1988, BHPP encountered a 10 m oil leg below a 20 m gas column in its Montara-1 well.||||||
12126|Montara Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Oxfordian|Oxfordian|Swan Group. Underlies the Lower Vulcan Formation, overlies the Plover Formation. Mount Ashmore Dome. Shallow marine sandstone. Mis-spelt as Montana in Fig.2.||||||
12126|Montara Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes heterolithic fine-grained yellow/buff sandstone and dark grey siltstone; highly bioturbated; ocassional reddish brown nodules/diagenetic overprint?|
12126|Montara Formation|67200|5|Briefly described|app 2 p7||||||||Heterolithic fine grained sandstone and siltstone; highly bioturbated.|
12126|Montara Formation|68135|5|Briefly described|p51 fig 2a|Late Jurassic|Middle Jurassic|Browse Basin.||||Is overlain by Vulcan Formation.||14-SEP-17
12126|Montara Formation|69297|6|Mentioned|p303, p305, p308, p309|Upper Jurassic|Upper Jurassic|Barcoo and Seringapatam Sub-basins of the Browse Basin. Deposited in a fluvial to deltaic environment.||Swan Group||Unconformably overlies the Ashmore Volcanics and the Plover Formation. Overlain by the Lower Vulcan Formation.||
12126|Montara Formation|69452|5|Briefly described|p36:15, 21-22|Jurassic|Jurassic|Bonaparte Basin.||Swan Group.||Equivalent to Elang Formation.||12-JUL-16
12126|Montara Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Overlies Plover Formation.||
12126|Montara Formation|70061|5|Briefly described|Regional geology; Fig.7, p6, p12, p17|Oxfordian|Callovian|See also Vulcan: Fig.2, p1-2. Bonaparte Basin; commercial petroleum reservoir. Contains mature marine, oil- and gas-prone source rocks.||Swan Group.||Overlies Plover Formation. Is overlain by Lower Vulcan Formation.|Retrogradational deltaic sandstones and transgressive marine shales.|12-JUL-16
12126|Montara Formation|70064|5|Briefly described|Northern Fig.2; p1-2. Yampi: Fig.2|Oxfordian|Callovian|See also Regional: Fig. 6; p6, p8-10. Central: Fig.2; p2. Caswell-Barcoo Sub-basins, Browse Basin. Potential source rock, and potential reservoirs in horsts and tilted fault-blocks. Oil and gas shows occur locally. Apparently includes [an informal? unit called] the Ichthys Formation: appears in Northern: p2 as Montara (Ichthys) Formation.||Swan Group.||Overlies Plover Formation or Ashmore Volcanics. Is overlain by Lower Vulcan Formation.|Prograding fan-delta systems.|12-JUL-16
12130|Montejinni Limestone|12891|5|Briefly described|p731, p733 Fig. 2|Late Cambrian|Middle Cambrian|Overlain by Hooker Creek Formation. Geological province: Wiso Basin. Sampled for hydrocarbon shows (p735). Fractured and vuggy carbonates are present and may have enhanced permeability.||||||07-FEB-11
12130|Montejinni Limestone|14019|5|Briefly described|p20|Middle Cambrian|Middle Cambrian|Fossiliferous unit.  Overlies the Antrim Plateau Volcanics.||||||
12130|Montejinni Limestone|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
12130|Montejinni Limestone|23410|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Bioclast, stylolitic, onkoid, mottled, ribbon and cryptomicrobial limestone and dolostone, minor siliciclastic and dolomitic mudstone; chert and evaporite nodules; local basal breccia; chertified at surface; fossiliferous. Geol. Prov: Wiso Basin.||||||02-NOV-05
12130|Montejinni Limestone|23733|5|Briefly described|p22, 23|Cambrian|Cambrian|||||||
12130|Montejinni Limestone|23770|5|Briefly described|p2 Fig. 1|Middle Cambrian|Middle Cambrian|Shallow marine to intertidal calcilutite, calcarentie, dolomite and clacareous siltstone.  Geological Province: Wiso Basin||||||
12130|Montejinni Limestone|23821|5|Briefly described|p244|||||||||14-NOV-06
12130|Montejinni Limestone|23981|6|Mentioned|p65|||Geological Province: South-eastern Wiso Basin.||||||14-FEB-07
12130|Montejinni Limestone|24122|3|Fully described|p13|Cambrian|Cambrian|Unconformably overlies Antrim Plateau Volcanics. Approximately 60m. thick.  Geological Province: Wiso Basin.||||||
12130|Montejinni Limestone|24297|4|Described|p19|Cambrian|Cambrian|Maximum thickness: 151m.  Unconformably overlies Antrim Plateau Volcanics. Geological Province: Wiso Basin.||||||
12130|Montejinni Limestone|24298|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, dolostone, mudstone, breccia, calcilutite, calcarenite.||||||19-OCT-05
12130|Montejinni Limestone|24300|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group.   Geological Province: Wiso Basin||||||07-NOV-06
12130|Montejinni Limestone|24303|3|Fully described|p39|Ordian-Early Templetonian|Ordian-Early Templetonian|Geological Province: Wiso Basin. Maximum Thickness: 151m. Correlates with the Tindall Limestone and Gum Ridge Formation. See also p63 Appendix.||||||04-DEC-12
12130|Montejinni Limestone|24304|5|Briefly described|Map legend|Cambrian|Cambrian|Limestone and dolostone; minor fine-grained sandstone and siliciclastic mudstone; fossiliferous; chert and nodular evaporitic pseudomorphs; silicified outcrop, recessive.||||||17-OCT-05
12130|Montejinni Limestone|28255|5|Briefly described|Summary|||Overlies Antrim Plateau Volcanics in the east. Correlated with Headleys Limestone. Geological Province: Daly River and Wiso Basins.||||||15-JUN-05
12130|Montejinni Limestone|29591|6|Mentioned|p107|||||||||
12130|Montejinni Limestone|30003|4|Described|p11, p14|Middle Cambrian|Middle Cambrian|Basal unit in the Wiso Basin.  Equivalent in part to Tindall Limestone in the Daly River Basin. Overlies the Antrim Plateau Volcanics.||||||19-APR-05
12130|Montejinni Limestone|30004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31412|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31413|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31637|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|31917|5|Briefly described|p32|||See Fig.3.||||||
12130|Montejinni Limestone|32175|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|32775|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||02-DEC-04
12130|Montejinni Limestone|33022|6|Mentioned|p271|||||||||
12130|Montejinni Limestone|33164|6|Mentioned|p87|||||||||
12130|Montejinni Limestone|33373|3|Fully described|Table 3|||p12.||||||07-NOV-06
12130|Montejinni Limestone|33374|4|Described|p13|||||||||
12130|Montejinni Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
12130|Montejinni Limestone|34051|5|Briefly described|Table 1|||L.- M.Camb. See also pp4,6 -11.||||||07-NOV-06
12130|Montejinni Limestone|34052|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|34438|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|34439|5|Briefly described|Table 1|||Middle Cambrian||||||
12130|Montejinni Limestone|34440|5|Briefly described|Table 1|||M.Camb.||||||
12130|Montejinni Limestone|34810|5|Briefly described|p8|||Does not outcrop in sheet area.||||||07-NOV-06
12130|Montejinni Limestone|35125|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|35224|4|Described|Table 1|||See also p5.||||||07-NOV-06
12130|Montejinni Limestone|35227|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|35229|4|Described|Table.1|||||||||
12130|Montejinni Limestone|35231|4|Described|Table.1|||||||||
12130|Montejinni Limestone|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
12130|Montejinni Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
12130|Montejinni Limestone|39210|6|Mentioned|p48|||||||||
12130|Montejinni Limestone|39523|6|Mentioned|p96|||||||||
12130|Montejinni Limestone|41864|6|Mentioned|p157|||In Wiso Basin||||||
12130|Montejinni Limestone|42059|4|Described|p135|||See also Fig.2||||||
12130|Montejinni Limestone|42504|6|Mentioned|p77|||||||||
12130|Montejinni Limestone|44113|5|Briefly described|p240|Middle Cambrian|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 78m.||||||
12130|Montejinni Limestone|44411|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
12130|Montejinni Limestone|44965|14|Not recorded|Not recorded|||||||||25-JAN-18
12130|Montejinni Limestone|45022|6|Mentioned|p.102||Middle Cambrian|||||||
12130|Montejinni Limestone|45064|3|Fully described|Table 1|||See also p19.||||||07-NOV-06
12130|Montejinni Limestone|45148|2|Defined|p9|Middle Cambrian|Middle Cambrian|Also mentioned p2.||||||07-NOV-06
12130|Montejinni Limestone|45155|6|Mentioned|Fig.8|||||||||
12130|Montejinni Limestone|45168|6|Mentioned|p6|||||||||
12130|Montejinni Limestone|47044|6|Mentioned|p191|||||||||
12130|Montejinni Limestone|48942|6|Mentioned|p73|||Strat. table.||||||
12130|Montejinni Limestone|48950|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12130|Montejinni Limestone|50353|5|Briefly described|Map Legend|Ordian-Early Templetonia|Ordian-Early Templetonia|Grey bioclast, styolitic, onkoid, mottled, ribbon and cryptomicrobial limestone and dolostone, minor maroon siliciclastic and yellow-grey dolomitic mudstone;chert and evaporite nodules; local basal breccia; chertified at surface, fossiliferous.||||||04-JUN-04
12130|Montejinni Limestone|60672|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Limestone, dolostone, calcareous mudstone and siltstone. Geological Province incorrectly shown as Ord Basin. Should be Wiso Basin||||||14-NOV-06
12130|Montejinni Limestone|60684|2|Defined|p48-49 Appendix, p16-17||Ordian-Early Templetonian|Unconformably overlies Antrim Plateau Volcanics; conformably overlain by Hooker Creek Formation and unconformably by Point Wakefield beds where former is absent. Age is probably Ordian- Early Templetonian. Max. thickness: 151.2m. Geol.Prov: Wiso Basin.||||||25-JAN-18
12130|Montejinni Limestone|60685|3|Fully described|p3 Fig. 2, p1|Cambrian|Cambrian|Consists of two limestone intervals seperated by mudstone. Overlies Antrim Plateau Volcanics. Max. Thickness: 151m. Geological Province: Wiso Basin. Lateral correlative of Tindall Limestone and Gum Ridge Formation.||||||
12130|Montejinni Limestone|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Wiso Basin. Faunal links with Antarctica.||||||
12130|Montejinni Limestone|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Wiso Basin (NT).||||||07-FEB-11
12130|Montejinni Limestone|62790|5|Briefly described|p207|Middle Cambrian|Middle Cambrian|Eastern Wiso Basin. Contains fossils of Bradoria alaris, and Parahoulongdongella? Sp. (Kruse, 1998, Fig.24), the only Ordian or early Templetonian representative of the Hipponicharionidae in Australia.||||||
12130|Montejinni Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Wiso Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
12130|Montejinni Limestone|64068|6|Mentioned|p225|||Wiso Basin. Correlated with Narpa Group.||||||
12130|Montejinni Limestone|64443|6|Mentioned|p40.|||Of Wiso Basin. Correlative of Barkly Group, Georgina Basin.||||||
12130|Montejinni Limestone|64780|5|Briefly described|p62 Fig.3 |Cambrian|Cambrian|||||||
12130|Montejinni Limestone|65239|5|Briefly described|p2-3|Middle Cambrian|Middle Cambrian|Conformably overlain by Point Wakefield beds. Geological province: Wiso Basin. Shallow, epeiric sea deposits.||||||04-JUN-09
12130|Montejinni Limestone|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Wiso Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
12130|Montejinni Limestone|65345|5|Briefly described|pp3-4, p6 Fig.5, p8. |Middle Cambrian|Middle Cambrian|Wiso Basin. Over 150 m thick. Contains a 15 m-thick phosphatic zone which is promising for further exploration. Shallow epeiric sea deposits.||||Is overlain by Hooker Creek Formation.|Limestone, dolostone, dolomitic limestone, calcareous mudstone and siltstone, commonly with abundant chert nodules.|
12130|Montejinni Limestone|67352|6|Mentioned|p19|Middle Cambrian|Middle Cambrian|Wiso Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
12130|Montejinni Limestone|69437|5|Briefly described|p22:10-11, 15-16|Series 2|Series 2|Wiso Basin, Centralian B Superbasin. Sequence 1. Shallow-marine and lesser peritidal deposits. Has potential as a petroleum source and reservoir rock.||||Is overlain by Hooker Creek Formation.|Limestone, dolostone and minor siliciclastic rocks.|12-JUL-16
12130|Montejinni Limestone|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Wiso 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
12130|Montejinni Limestone|69439|6|Mentioned|p24:10|||Wiso Basin. The interval Montejinni Limestone-Lothari Hill Sandstone is correlated with the Walbiri Dolostone of the Ngalia Basin.||||||12-JUL-16
12130|Montejinni Limestone|69443|6|Mentioned|p28:21|||Wiso Basin.||||Correlated with Gum Ridge Formation.||12-JUL-16
12130|Montejinni Limestone|69445|5|Briefly described|p30:5, 11, 17|Middle Cambrian|Middle Cambrian|Randal and Brown (1967). Wiso Basin. Associated with the Crowsons Prospect copper occurrence.||||Unconformably overlies Antrim Plateau Volcanics (Kalkarindji Suite).||12-JUL-16
12130|Montejinni Limestone|69446|6|Mentioned|p31:2-3|||Wiso Basin. Probably continuous with Tindall Limestone under cover.||||||12-JUL-16
12130|Montejinni Limestone|69447|4|Described|p32:2-5, 7-9|Middle Cambrian|Middle Cambrian|Traves (1955). Oldest unit in the Wiso Basin. Peritidal to restricted marine deposits. Up to 151m thick. Crops out as a rugged dissected terrace flanking a plateau, and as isolated mesas or sparse low rises or boulder fields. The main producing aquifer in the western Wiso Basin. Fossiliferous: trilobites including Redlichia, bradoriides, brachiopods, hyoliths, molluscs, echinoderm plates, sponge spicules and chancelloriids. Has strong species-level similarity to correlative faunas of Linnekar Limestone and Panton Formation (Ord Basin) and Tindall Limestone (Daly Basin). Associated with the Kunayangku, Lady Judith and Warrego West phosphate prospects. The Crowsons (copper) Prospect occurs at/near the contact with Antrim Plateau Volcanics. Has fair to good petroleum source rock potential; hydrocarbon shows have been recorded. Has good potential as a reservoir.||||Unconformably overlies Antrim Plateau Volcanics. Is overlain conformably and gradationally by Hooker Creek Formation and unconformably by Point Wakefield beds.|Limestone and dolostone (including microbial (dolo)laminite and mottled, bioclast, oncoid and ribbon types), maroon-green siltstone; minor dolomitic quartz sandstone; local basal polymict breccia; nodular evaporites, hot and cold seep structures.|12-JUL-16
12130|Montejinni Limestone|69448|6|Mentioned|p33:3|||Wiso Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
12130|Montejinni Limestone|69458|5|Briefly described|p42:20|Middle Cambrian|Middle Cambrian|Wiso Basin.||||Overlies Antrim Plateau Volcanics. Is overlain unconformably by Camfield beds.||14-SEP-18
12130|Montejinni Limestone|69673|5|Briefly described|ix, p142, p145, p146 fig 117|Cambrian|Cambrian|Minor hydrocarbon shows have been noted in this unit. Up to 151m thick. Contains marine fossils and stromatolites.||||Overlain by the Hooker Creek Formation|Fractured and vuggy limestone, dolostone, siltstone and minor dolomitic quartz sandstone.|
12130|Montejinni Limestone|70380|6|Mentioned|p745|Stage 5|Stage 4|Wiso Basin.||||||
12130|Montejinni Limestone|70752|6|Mentioned|p129|||Wiso Basin. Brachiopod systematic palaeontological descriptions.||||||
12130|Montejinni Limestone|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin. The two facies are mapped separately.|||||Mudstone and argillaceous limestone, siliceous breccia at base; limestone, dolostone.|
12130|Montejinni Limestone|70854|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin.|||||Limestone, dolostone, calcareous mudstone and siltstone.|
12130|Montejinni Limestone|70855|5|Briefly described|Map legend.|Cambrian|Cambrian|Wiso Basin.|||||Limestone, dolostone, calcareous mudstone and siltstone. Three facies are mapped separately: limestone, dolostone; mudstone and argillaceous limestone, siliceous breccia at base; calcilutite, calcarenite, dolostone.|
12130|Montejinni Limestone|70968|5|Briefly described|p112|Middle Cambrian|Middle Cambrian|Wiso Basin. Kennewell and Huleatt (1980) assigned the Lake Woods beds (at that stage mapped as Gum Ridge Formation) to this unit; subsequently reassigned to Renner Group by Hussey et al. (2001).||||Unconformably overlies Lake Woods beds.||
12130|Montejinni Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, dolostone|
12130|Montejinni Limestone|71754|14|Not recorded|p199|||SF52-4.||||||
12130|Montejinni Limestone|73083|6|Mentioned|p12, p14, p24-25, p30, p38, p49|Cambrian|Cambrian|Wiso Basin.||||||
12134|Montescue Group|41028|6|Mentioned|p227|||||||||
12179|Moogooloo Sandstone|12733|6|Mentioned|p555.|||Merlinleigh Sub-basin. Has excellent reservoir characteristics.||||||
12179|Moogooloo Sandstone|14228|5|Briefly described|p3 tab 1, p7, p8, p18, p21|Lower Permian|Lower Permian|Fluvial-deltaic. A primary reservoir objective.||Wooramel Group||Overlies/grades into Cordalia Formation. Overlain by Billidee Formation (conformably).||05-OCT-16
12179|Moogooloo Sandstone|22817|4|Described|p4|Early Permian|Early Permian|||||||
12179|Moogooloo Sandstone|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
12179|Moogooloo Sandstone|23310|5|Briefly described|Map legend|Artinskian|Artinskian|Of  Wooramel Group.||||||
12179|Moogooloo Sandstone|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Wooramel Group.||||||
12179|Moogooloo Sandstone|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Wooramel Group.||||||
12179|Moogooloo Sandstone|23403|4|Described|p8|Early Permian|Early Permian|Of Wooramel Group.  Consists of commonly well sorted, fine- to coarse-grained quartz sandstone.||||||24-NOV-09
12179|Moogooloo Sandstone|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Parent: Wooramel Group.   Quartzose or feldspathic sandstone and siltstone; minor claystone, and carbonaceous shale.||||||
12179|Moogooloo Sandstone|23726|5|Briefly described|p12|Early Permian|Early Permian|Of Wooramel Group. Overlying unit Billidee Formation. Underlying unit Callytharra Formation. Geological Province: Carnarvon Basin.||||||
12179|Moogooloo Sandstone|23815|4|Described|p280-282|Artinskian|Artinskian|Formerly known as the "Moogooloo Division". Geological Province: Merlinleigh Sub-basin. Of the Wooramel Group. Underlying unit: Cordalia Greywacke (conformable). Overlying unit: Billidee Formation (conformable). Max. thickness: 128 m.||||||27-APR-05
12179|Moogooloo Sandstone|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Wooramel Group.||||||
12179|Moogooloo Sandstone|24059|5|Briefly described|p147|Permian|Permian|Of Wooramel Group. Geological Province: Carnarvon Basin.||||||
12179|Moogooloo Sandstone|24114|5|Briefly described|p8|||Of Wooramel Group. Geological Province: Carnarvon Basin.||||||
12179|Moogooloo Sandstone|24410|5|Briefly described|p137|Permian|Permian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||24-NOV-09
12179|Moogooloo Sandstone|31561|4|Described|p35|||See also P9||||||
12179|Moogooloo Sandstone|32113|4|Described|p47|||re sedimentology||||||
12179|Moogooloo Sandstone|32648|6|Mentioned|p32|||Wooramel Gp.||||||
12179|Moogooloo Sandstone|33594|4|Described|p38|||||||||
12179|Moogooloo Sandstone|33710|6|Mentioned|Fig.1|||||||||
12179|Moogooloo Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
12179|Moogooloo Sandstone|34532|6|Mentioned|p225|||Wooramel Gp.||||||
12179|Moogooloo Sandstone|35105|6|Mentioned|Fig.66|||||||||
12179|Moogooloo Sandstone|35282|6|Mentioned|p23|||||||||
12179|Moogooloo Sandstone|36257|6|Mentioned|Table 2.1|||||||||
12179|Moogooloo Sandstone|36890|3|Fully described|p281|||||||||
12179|Moogooloo Sandstone|36902|6|Mentioned|p22|||||||||
12179|Moogooloo Sandstone|37295|6|Mentioned|p53|||||||||
12179|Moogooloo Sandstone|37920|6|Mentioned|p457|||||||||
12179|Moogooloo Sandstone|38482|6|Mentioned|p22|||||||||
12179|Moogooloo Sandstone|38493|4|Described|p35|||||||||
12179|Moogooloo Sandstone|38494|4|Described|p29|||||||||
12179|Moogooloo Sandstone|39370|5|Briefly described|p35|||See also P3||||||
12179|Moogooloo Sandstone|39427|4|Described|Table 1|||||||||
12179|Moogooloo Sandstone|40336|6|Mentioned|p18|||||||||
12179|Moogooloo Sandstone|40339|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
12179|Moogooloo Sandstone|40340|6|Mentioned|Table 2|||||||||
12179|Moogooloo Sandstone|40343|6|Mentioned|p11|||||||||
12179|Moogooloo Sandstone|40617|6|Mentioned|Fig.1|||||||||
12179|Moogooloo Sandstone|41271|3|Fully described|p82|||||||||
12179|Moogooloo Sandstone|41436|6|Mentioned|p42|||||||||
12179|Moogooloo Sandstone|41438|6|Mentioned|p104|||||||||
12179|Moogooloo Sandstone|42116|4|Described|p32|||||||||
12179|Moogooloo Sandstone|42734|5|Briefly described|map legend|Permian||||||||
12179|Moogooloo Sandstone|43255|5|Briefly described|map legend||Artinskian|of Wooramel Group.||||||
12179|Moogooloo Sandstone|43256|5|Briefly described|5-22||Permian|of Wooramel Group||||||
12179|Moogooloo Sandstone|43835|5|Briefly described|Map Legend||Artinskian|||||||
12179|Moogooloo Sandstone|44344|14|Not recorded|p.4,10,19,22,24|Permian|Artinskian|Artinskian (Permian). (G50-1). opp.4, map.||||||
12179|Moogooloo Sandstone|44345|14|Not recorded|map legend||Artinskian|||||||
12179|Moogooloo Sandstone|44532|4|Described|p.6,7,15, map|||Aquifer. (G50-5).||||||
12179|Moogooloo Sandstone|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
12179|Moogooloo Sandstone|44994|6|Mentioned|Fig.7|||Correlation. Permian.||||||
12179|Moogooloo Sandstone|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group.||||||01-JUN-06
12179|Moogooloo Sandstone|45016|2|Defined|p.82-88||Artinskian|Tb, p46,67,68,Fig.65,74, p.51,75,77-81,91-94,96,98,99,101,106,111,112,123,137,140. (F50-13,G50-1,2,5,6).||||||
12179|Moogooloo Sandstone|45168|6|Mentioned|p6|||||||||
12179|Moogooloo Sandstone|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
12179|Moogooloo Sandstone|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.||Lower unit in Wooramel Group.||Is overlain by Billidee Formation.|Fine- to very coarse-grained quartz sandstone; minor siltstone and granule to pebble conglomerate.|
12179|Moogooloo Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes light tan grey coarse-grained sandstone with minor carbonaceous flecks.|
12179|Moogooloo Sandstone|67200|5|Briefly described|p7 fig 5, p48, p55, app 2 p6|Kungurian|Artinskian|Thermal conductivity of 4.76 W/mK||Wooramel Group||Unconformably overlies Cordalia Formation, overlain by Billidee Formation|Coarse grained sandstone with minor carbonaceous flecks  and siltstone with coal and trough cross beds.|
12179|Moogooloo Sandstone|67373|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.||Unit in Wooramel Group.|||Fine- to very coarse-grained quartz sandstone; minor siltstone and granule to pebble conglomerate.|
12179|Moogooloo Sandstone|67977|5|Briefly described|p481 Fig. 2|Artinskian|Artinskian|Geol. Prov: Merlinleigh Sub-basin, Southern Carnarvon Basin||Wooramel Group||overlies Cordalia Formation||
12179|Moogooloo Sandstone|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Wooramel Group.||Overlain by the Billidee Formation. Underlain by the Callytharra Formation.|Comprises fine to very coarse grained quartz sandstone; minor siltstone and granule to pebble conglomerate.|
12179|Moogooloo Sandstone|69166|4|Described|geologyp_lut.csv|Artinskian|Artinskian|||Wooramel Group|||Fine to very coarse grained quartz sandstone; minor siltstone and granule to pebble conglomerate|
12179|Moogooloo Sandstone|70138|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.||Wooramel Group.|||Fine- to very coarse-grained quartz sandstone; minor siltstone and granule to pebble conglomerate.|
12179|Moogooloo Sandstone|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Southern Carnarvon Basin.||Wooramel Group||Overlies the Cordalia Formation. Overlain by the Billidee Formation.||
12179|Moogooloo Sandstone|70795|4|Described|100k_geologyp_lut.csv|Artinskian|Artinskian|Also 100k_interpgeop_lut.csv|290-283 Ma|Wooramel Group|||Fine to very coarse grained quartz sandstone; minor siltstone and granule to pebble conglomerate.|
12179|Moogooloo Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, claystone, shale, sandstone|
12179|Moogooloo Sandstone|72910|4|Described|p4, p7-9, p14-16, p18-24, p30-32, p34.|Artinskian|Artinskian|Thickness 30-115m. Restricted to Merlinleigh Sub-basin. See also  p39, p41-42. Type section is located at the South end of Gooch Range, 23d51m10sS, 114d48m30sE. p39 says laterally [equivalent to] Callytharra Formation. Rare fossils. Fluvial to delta front environment suggested.||Wooramel Group.||Conformably overlies Cordalia Formation, Callytharra Formation and laterally equivalent to lower Keogh Formation. Interfingers with overlying Billidee Formation.|Fine to coarse quartz sandstone, minor siltstone, conglomerate.|
12181|Moogooree Limestone|12471|6|Mentioned|p475 Fig.2, p483.|Early Carboniferous|Early Carboniferous|Appears to have little hydrocarbon reservoir potential.||||Is overlain by Quail Formation.||
12181|Moogooree Limestone|12733|6|Mentioned|p554 Fig.2.|Early Carboniferous|Early Carboniferous|Tournaisian.||||Overlies Willaradie Formation. Is overlain by Williambury Sandstone.||
12181|Moogooree Limestone|13615|3|Fully described|p4, 12, 15-16, 34, 42, 55, 78, 80, 103|Visean|Tournaisian|Peedamullah Shelf. Spores and Pollen zone provided. Interesected in Amber 1. Type section occcurs Southeast of Williambury Homestead 23deg54'S 115deg10'40"E. Contains fossil algae, corals, echinoderms, brachiopods. Deposited in a nearshore to intertidal environment. See also p118.|c. 354 Ma|||Disconformably overlies the Gneudna Formation. Overlain by the Quail Formation probably conformably.|Limestone and dolostone ranging from mudstone to boundstone and minor calcareous sandstone.|07-FEB-19
12181|Moogooree Limestone|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18|Tournaisian|Famennian|Merlinleigh Sub-basin. Possible seal for Munabia Formation.||||Overlies Munabia and Willaraddie Formations. Is overlain by Quail and Williambury Formations.||
12181|Moogooree Limestone|22814|5|Briefly described|fig2|Early Carboniferous|Late Devonian|||||||
12181|Moogooree Limestone|23311|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|||||||
12181|Moogooree Limestone|23312|5|Briefly described|map legend|Early Carboniferous|Tournaisian|||||||
12181|Moogooree Limestone|23403|4|Described|p7|Early Carboniferous|Middle Devonian|Consists dominantly limestone and dolomite with minor siliciclastic and evaporative horizons.  Geological Province: Gascoyne Complex.||||||15-NOV-12
12181|Moogooree Limestone|23726|5|Briefly described|p36 Fig 11|Early Carboniferous|Early Carboniferous|Underlying unit Munabia Sandstone. Geological Province: Carnarvon Basin.||||||
12181|Moogooree Limestone|23815|4|Described|p276, 277|Tournaisian|Tournaisian|Geological Province: Carnarvon Basin. Underlying unit: Willaraddie Formation (disconformable). Overlying unit: Williambury Formation (conformable) and Lyons Group (unconformable). Max. thickness: 400 m. Is richly fossiliferous.||||||27-APR-05
12181|Moogooree Limestone|24059|5|Briefly described|p146|Early Carboniferous|Early Carboniferous|Geological Province: Carnarvon Basin.||||||
12181|Moogooree Limestone|24390|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
12181|Moogooree Limestone|29548|6|Mentioned|p226|||||||||
12181|Moogooree Limestone|30875|6|Mentioned|p10|||Carboniferous.||||||
12181|Moogooree Limestone|31561|5|Briefly described|p34|||See also P33. Early Carboniferous.||||||
12181|Moogooree Limestone|31706|6|Mentioned|p651|||L.Carboniferous correlation chart||||||
12181|Moogooree Limestone|32648|6|Mentioned|p32|||Tournaisian||||||
12181|Moogooree Limestone|32865|6|Mentioned|p477|||L.Carb.||||||
12181|Moogooree Limestone|33386|6|Mentioned|Fig.7|||||||||
12181|Moogooree Limestone|33453|5|Briefly described|p69|||Carb.||||||
12181|Moogooree Limestone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
12181|Moogooree Limestone|34287|6|Mentioned|p108|||||||||
12181|Moogooree Limestone|34838|6|Mentioned|p4|||||||||
12181|Moogooree Limestone|34846|6|Mentioned|Fig.3|||||||||
12181|Moogooree Limestone|35282|6|Mentioned|p1|||||||||
12181|Moogooree Limestone|35981|5|Briefly described|p133|||See also P134.||||||
12181|Moogooree Limestone|36257|6|Mentioned|Table 2.1|||||||||
12181|Moogooree Limestone|36890|3|Fully described|p277|||||||||
12181|Moogooree Limestone|38770|6|Mentioned|Fig.1|||||||||
12181|Moogooree Limestone|39427|4|Described|Table 1|||||||||
12181|Moogooree Limestone|40617|6|Mentioned|p4|||Mention Fig.1||||||
12181|Moogooree Limestone|40992|6|Mentioned|Fig.8|||||||||
12181|Moogooree Limestone|41271|3|Fully described|p55|||||||||
12181|Moogooree Limestone|41438|6|Mentioned|p102|||||||||
12181|Moogooree Limestone|41441|5|Briefly described|p151|||||||||
12181|Moogooree Limestone|41443|4|Described|p159|||||||||
12181|Moogooree Limestone|41444|6|Mentioned|Fig.4|||||||||
12181|Moogooree Limestone|41839|4|Described|p19|||||||||
12181|Moogooree Limestone|42116|4|Described|p25|||See also Fig.9, 10||||||
12181|Moogooree Limestone|42547|4|Described|p88|||||||||
12181|Moogooree Limestone|42994|6|Mentioned|p12|||||||||
12181|Moogooree Limestone|43566|6|Mentioned|p413|||||||||
12181|Moogooree Limestone|44344|14|Not recorded|p.3,5-7,24,opp.4,map||Early Carboniferous|L.Carb., probably Tournaisian.||||||
12181|Moogooree Limestone|44345|14|Not recorded|map legend||Early Carboniferous|Lower Carboniferous.||||||
12181|Moogooree Limestone|44537|14|Not recorded|map legend||Early Carboniferous|Lower Carboniferous.||||||
12181|Moogooree Limestone|44657|14|Not recorded|p.5,7,8|||||||||
12181|Moogooree Limestone|44993|14|Not recorded|p.12,42|||Camarateochia.||||||
12181|Moogooree Limestone|44994|5|Briefly described|p9|||Correlation Fig.6||||||
12181|Moogooree Limestone|45015|2|Defined|p63-67, p53 Fig.21, map legend|Early Carboniferous|Early Carboniferous|Dominated by calcarenite, friable in the lower section; recrystallised, siliceous and hard in upper part. Unconformable on Willaraddie Fm. or Munabia Sandstone; conformable below  Williambury Formation or unconformably by Lyons Group. Max.thick: 1260ft.||||||31-MAY-06
12181|Moogooree Limestone|45016|14|Not recorded|p.9,21,29||Early Carboniferous|L.Carboniferous.||||||
12181|Moogooree Limestone|45041|6|Mentioned|Fig.45|||L.Carb.||||||
12181|Moogooree Limestone|45063|6|Mentioned|p18|||Se also P30 & Fig. 9. Carb.||||||
12181|Moogooree Limestone|45097|5|Briefly described|p22|||Tournaisian. Correlation chart||||||
12181|Moogooree Limestone|45143|6|Mentioned|p29|||||||||
12181|Moogooree Limestone|46978|4|Described|p106|||||||||
12181|Moogooree Limestone|48831|14|Not recorded|p.60,66,67,69|||||||||
12181|Moogooree Limestone|48971|6|Mentioned|p42|||||||||
12181|Moogooree Limestone|49942|5|Briefly described|p4 Fig.3|Carboniferous|Carboniferous|Geological Province: Merlinleigh Sub-basin.||||||03-FEB-05
12181|Moogooree Limestone|50085|5|Briefly described|p19 Fig. 10|Carboniferous|Late Devonian|Geological Province: Southern Carnarvon Basin.||||||
12181|Moogooree Limestone|60384|5|Briefly described|p244, p243 Fig 2a||Early Carboniferous|Merlinleigh Sub-Basin, Southern Carnarvon Basin. Platform carbonate.|||||Platform carbonate|
12181|Moogooree Limestone|60725|5|Briefly described|p29 Fig.2, p30, p36 Fig.6. |Tournaisian|Tournaisian||||||Shallow-marine carbonates.|
12181|Moogooree Limestone|61023|5|Briefly described|p34 Fig. 14|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
12181|Moogooree Limestone|61958|5|Briefly described|Map sheet 1|Early Carboniferous|Early Carboniferous|||||||
12181|Moogooree Limestone|64580|6|Mentioned|map legend|||Carboniferous succession, Southern Carnarvon Basin.||||||15-DEC-08
12181|Moogooree Limestone|64972|6|Mentioned|p617 Fig. 5|Early Carboniferous|Early Carboniferous|||||||
12181|Moogooree Limestone|67200|5|Briefly described|p7 fig 5,|Carboniferous|Carboniferous|||||Overlies Willaraddie Formation, overlain by Quail Formation, Williambury Formation|Parallel bedded limestone.|
12181|Moogooree Limestone|69011|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlain by the Williambury Formation. Underlain by the Willaraddie Formation.|Comprises limestone and dolomite (wackestone, packstone, grainstone, and boundstone); minor calcareous sandstone.|24-APR-14
12181|Moogooree Limestone|69029|6|Mentioned|p326|Tournasian|Tournasian|Of onshore Carnarvon Basin.||||Overlain by Williambury Sandstone. Underlain by Willaradie Formation.||
12181|Moogooree Limestone|69182|5|Briefly described|Ch3 p8, Ch3 p10-p11|Early Carboniferous|Early Carboniferous|Carnarvon Basin. Deposited in shallow-marine conditions. See also Ch3 p23-p26, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Overlies the Willaraddie Formation. Overlain by the Williambury Formation.|Limestone.|
12181|Moogooree Limestone|69297|5|Briefly described|p249|Tournaisian|Tournaisian|Gascoyne Sub-basin of the Southern Carnarvon Basin.||||Overlies the Munabia Sandstone. Overlain by the Quail Limestone.|Limestones.|
12181|Moogooree Limestone|70138|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlies Willaraddie Formation. Is overlain by Williambury Formation.|Limestone and dolomite (wackestone, packstone, grainstone and boundstone); minor calcareous sandstone.|
12181|Moogooree Limestone|70795|4|Described|100k_geologyp_lut.csv|Tournaisian|Tournaisian|Also 100k_interpgeop_lut.csv|359-347 Ma||||Limestone and dolomite (wackstone, packstone, grainstone, and boundstone); minor calcareous sandstone.|
12181|Moogooree Limestone|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|||||||
12181|Moogooree Limestone|71146|5|Briefly described|p6, p27|Tournaisian|Tournaisian|Southern Carnarvon Basin. Hosts some sub-economic lead zinc deposits. Deposited in a shallow marine environment.||||Overlies the Willaraddie Formation. Overlain by the Williambury Formation.|Limestone and mudstone.|
12181|Moogooree Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone|
12181|Moogooree Limestone|72502|6|Mentioned|p23|||Contains the shark species Deihim mansureae (Trinajstic et al., 2014).||||||
12182|Moola Bulla Formation|22754|5|Briefly described|p5 Tb. 1, p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age 1835-1805 Ma.  Geological Province: Moola Bulla Basin.||||||07-NOV-08
12182|Moola Bulla Formation|23383|4|Described|p17, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Lamboo Complex.  Coarse feldspathic sandstone, pebble conglomerate, fine- to coarse-grained sandstone, siltstone, mudstone.  Age: 1820-1805Ma.  Max thickness 1350 m. Geol.Prov: Moola Bulla Basin. See also p6 Fig. 3.||||||07-NOV-08
12182|Moola Bulla Formation|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lithic quartz sandstone and granule to pebble conglomerate; minor argillite. Geological Province: Kimberely Basin.||||||07-NOV-08
12182|Moola Bulla Formation|23621|3|Fully described|p21|Statherian|Orosirian|See also page 10 table 1. Age: 1843-~1800 Ma. Overlying unit King Leopold Sandstone. Underlying unit Olympio Formation. Geological Province: Moola Bulla Basin. Max. thickness: 3000 m.||||||
12182|Moola Bulla Formation|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Moola Bulla Basin.||||||07-NOV-08
12182|Moola Bulla Formation|23809|5|Briefly described|p9|||Geological Province: Halls Creek Orogen.  Tentatively correlated with the Pargee Sandstone.||||||30-MAR-05
12182|Moola Bulla Formation|24173|3|Fully described|p22, p12 Tb.2|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by King Leopold Sandstone; unconformably overlies Olympio Formation. Geological Province: Moola Bulla Basin. Conformably overlies Koongie Park Formation in ANGELO to the west. Age: ~1843-1800Ma. May be a correlative of Speewah Group||||||07-NOV-08
12182|Moola Bulla Formation|30097|6|Mentioned|Fig.54|||Also 23,24||||||
12182|Moola Bulla Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12182|Moola Bulla Formation|32660|5|Briefly described|Table 3|||||||||
12182|Moola Bulla Formation|32728|5|Briefly described|p36|||||||||
12182|Moola Bulla Formation|36551|6|Mentioned|Table 10|||||||||
12182|Moola Bulla Formation|36885|4|Described|p176|||||||||
12182|Moola Bulla Formation|36902|6|Mentioned|p11|||||||||
12182|Moola Bulla Formation|37462|4|Described|Table4.III|||||||||
12182|Moola Bulla Formation|38482|6|Mentioned|Table 1|||||||||
12182|Moola Bulla Formation|38988|6|Mentioned|Fig.4|||||||||
12182|Moola Bulla Formation|42768|5|Briefly described|p6|||see also Fig.6||||||
12182|Moola Bulla Formation|44140|5|Briefly described|p293, p295-297, p299|Paleoproterozoic|Paleoproterozoic|More than 3000 m thick. Locally derived from the Lamboo Complex. Parent possibly Speewah Group.||||Unconformable between Halls Creek Group and King Leopold Sandstone. Correlated with Speewah Group.|Arkose, greywack, conglomerate, siltstone; fluvial.|07-MAR-18
12182|Moola Bulla Formation|44155|6|Mentioned|p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|Kimberley region.||||||
12182|Moola Bulla Formation|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Lithic quartz sandstone and granule to pebble conglomerate; minor argillite. Geological Province: Moola Bulla Basin.||||||07-NOV-08
12182|Moola Bulla Formation|44324|14|Not recorded|p.7||Carpentarian|Tb.1. (Carpentarian).||||||
12182|Moola Bulla Formation|44325|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
12182|Moola Bulla Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
12182|Moola Bulla Formation|45047|2|Defined|p73|Carpentarian|Carpentarian|||||||
12182|Moola Bulla Formation|60724|5|Briefly described|p18, p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Kimberley Group. Correlative of Speewah Group. See also p12.||||||07-NOV-08
12182|Moola Bulla Formation|61861|6|Mentioned|p16, Fig 2|||Halls Creek Orogen. Tentatively correlated with Pargee Sandstone of Tanami Region.|1835 Ma.|||||
12182|Moola Bulla Formation|63866|4|Described|p129-p130, p132, p137|||Eastern Zone, Halls Creek Orogen.||||Unconformably overlies the Koongie Park Formation. Unconformably overlain by the Kimberley Group. Possibly equivalent to the Red Rock Formation and Texas Downs Formation.|Fluvial or shallow marine deltaic sandstone and mudstone sequence.|
12182|Moola Bulla Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, mudstone, and granule to cobble conglomerate.||||||09-DEC-08
12182|Moola Bulla Formation|68078|6|Mentioned|p23|||Broadly similar to lower Kimberley Group, may be broadly coeval.||||||
12182|Moola Bulla Formation|69003|6|Mentioned|p19|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. See also reference to Moola Boola Formation (p5).||||||
12182|Moola Bulla Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Moola Bulla Basin|||Includes 4 unnamed members.||Lithic and lithic quartz sandstone, mudstone, and granule to cobble conglomerate.|03-AUG-15
12182|Moola Bulla Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.|||||Sandstone, lithic quartz sandstone, mudstone and granule to cobble conglomerate.|
12182|Moola Bulla Formation|69585|6|Mentioned|p4-5|Statherian|Statherian|Lamboo Province.||||Probable equivalent of the Kimberley Group.||
12182|Moola Bulla Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Mulla Bolla Basin. King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|2500-1600 Ma (Inferred)||||Sandstone and lithic quartz sandstone, mudstone, and granule to cobble conglomerate|
12182|Moola Bulla Formation|70154|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1600-2500 Ma||||Sandstone, mudstone and granule to cobble conglomerate, lithic sandstone, lithic quartz sandstone.|
12182|Moola Bulla Formation|70812|5|Briefly described|p6|Statherian|Orosirian|Central and Eastern zones of the Halls Creek Orogen, Lamboo Province.|c. 1800-1750 Ma|||||
12182|Moola Bulla Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
12182|Moola Bulla Formation|70851|5|Briefly described|p4, p11-p12|Paleoproterozoic|Paleoproterozoic|Central and Eastern zones, Lamboo Province. Rock properties are provided.|c. 1800-1750 Ma|||||
12182|Moola Bulla Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Mulla Bulla 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.|2500-1600 Ma (inferred)||||Sandstone, lithic quartz sandstone, mudstone, and granule to cobble conglomerate at base.|
12182|Moola Bulla Formation|71397|6|Mentioned|p5|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen.||||||
12182|Moola Bulla Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Moola Bulla Basin.|||||Sandstone, mudstone, and granule to cobble conglomerate.|
12201|Moolyella Suite|23807|5|Briefly described|p122|Archean|Archean|See also Moolyella Adamellite Suite.  Geological Province: Pilbara Craton.||||||07-NOV-08
12201|Moolyella Suite|24590|5|Briefly described|p40 Fig. 2.3|||In the centre of the Gneiss Complex of the Mount Edgar Granitoid Complex. Also referred to as Moolyella Adamellite Suite in text (p41).||||||07-FEB-11
12201|Moolyella Suite|41938|4|Described|p11|||||||||
12201|Moolyella Suite|69041|3|Fully described|p4, p9-p10, p18-p19|Mesoarchean|Paleoarchean|Pilbara Craton, of the Mount Edgar Igneous Complex (which is used in a province sense). Crops out over 55km^2 of rugged terrain and forms an irregular M shaped pluton. This suite is well exposed and has a relatively high topographic relief. Originally named the Moolyella Granite by De Laeter & Blockley (1972) later defined and named the Moolyella Adamellite by Hickman & Lipple (1975). De Laeter & Blockley (1972) dated the suite at 2613 +/- 93 Ma using Rb-Sr, while Collins & Gray (1990) dated it at 2804 +/- 62 via whole rock isochron. Monzogranite has a high K, U and Th radiometric counts and low magnetic susceptibility. This unit differs from the older surrounding granitoids.Chemically highly fractionated.|3213 (U-Pb, Hickmann, pers. Comm)||||Medium-grained, quartz-rich, biotite monzogranite with a sparsely developed quartz-feldspar porphyritic texture.|21-JUN-19
12201|Moolyella Suite|69167|6|Mentioned|GA_geochron.csv|Archaean|Archaean|||||||
12268|Moonyoonooka Sandstone|23816|4|Described|p243|Bajocian|Early Jurassic|Geological Province: Perth Basin. Of the Chapman Group. Underlying unit: Greenough Sandstone (disconformable). Overlying unit: Colalura Sandstone (disconformable). Max. thickness: 34 m.||||||16-DEC-04
12268|Moonyoonooka Sandstone|30948|6|Mentioned|Map legend|Lias|Lias|||||||
12268|Moonyoonooka Sandstone|31396|6|Mentioned|p1183|||See also P1184||||||
12268|Moonyoonooka Sandstone|31561|6|Mentioned|p18|||See also section P12.||||||
12268|Moonyoonooka Sandstone|31910|6|Mentioned|p21|||||||||
12268|Moonyoonooka Sandstone|32648|6|Mentioned|p32|||Champion Bay Gp.||||||
12268|Moonyoonooka Sandstone|32649|4|Described|p24|||See also Table 1||||||
12268|Moonyoonooka Sandstone|33022|6|Mentioned|p256|||See also palaeomagnetism P265||||||
12268|Moonyoonooka Sandstone|33166|6|Mentioned|p63|||Refers Arkell & Playford (1954)||||||
12268|Moonyoonooka Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
12268|Moonyoonooka Sandstone|35282|6|Mentioned|Fig.2|||||||||
12268|Moonyoonooka Sandstone|36257|6|Mentioned|Table 2.1|||||||||
12268|Moonyoonooka Sandstone|36293|2|Defined|p142|Early Jurassic|Early Jurassic|||||||
12268|Moonyoonooka Sandstone|36890|3|Fully described|p243|||||||||
12268|Moonyoonooka Sandstone|38444|6|Mentioned|p300|||||||||
12268|Moonyoonooka Sandstone|44144|4|Described|p505-506 Tb.4-21|Aalenian|Early Jurassic|Type Section: Moonyoonooka 28o47'18''S 114o47'36''E. 34m thick fluvial deposits.||Chapman Group.||Conformably overlies Greenough Sandstone. Disconformably overlain by Colalura Sandstone and Newmarracarra Limestone.|White, grey, brown or red, fine- to very fine-grained feldspathic sandstone and arkose; carbonaceous shale and conglomerate lenses.|
12268|Moonyoonooka Sandstone|48857|14|Not recorded|p.10|||||||||
12268|Moonyoonooka Sandstone|61811|4|Described|pp29-31, pp34-35, p64.|Early Jurassic|Early Jurassic|Type section on Moonyoonooka property east of Geraldton is described; further details in Appendix 1. 25 m thick. Upper erosional contact is a significant sequence boundary.||Upper unit in Chapman Group.||Overlies Greenough Sandstone; locally overlies Northampton Complex basement. Is overlain by Champion Bay Group.|Very fine-grained and feldspathic sandstone with minor carbonaceous shale and basal sandy conglomerate.|
12268|Moonyoonooka Sandstone|64635|5|Briefly described|p16|Toarcian|Toarcian|Type section on the Moonyoonooka property east of Geraldton.||Of the Chapman Group.||Overlies the Greenough Sandstone. Is overlain by Champion Bay Group.|Very fine grained and feldspathic with minor carbonaceous shale and conglomerate.|
12271|Moora Group|22716|5|Briefly described|table4, p238|Tonian|Stenian|Age: 1000Ma. Western Margin of Yilgarn Craton.||||||
12271|Moora Group|23174|6|Mentioned|p9|||||||||
12271|Moora Group|23761|6|Mentioned|p4 Fig. 2|Proterozoic|Proterozoic|Consists of lithified sandstone, arkose, siltstone and volcanic rocks.  Geological Province: Yilgarn Block.  See also p12.||||||
12271|Moora Group|23762|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||23-DEC-09
12271|Moora Group|23788|5|Briefly described|p5|Proterozoic|Proterozoic|Includes the former Billeranga Group.  Geological Province: Yilgarn Craton.||||||
12271|Moora Group|24160|5|Briefly described|p20, 23|Proterozoic|Proterozoic|Pinjarra Orogen. Bentonite deposits occur in Quaternary sediments overlying this unit, at Marchagee and Watheroo.|||Includes Billeranga and Coomberdale Subgroups.|||
12271|Moora Group|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Broadly comprises a 'weakly deformed immature fluviatile-alluvial fan-basin margin' which unconformably overlies the Archaean Yilgarn Craton. See also p141 Fig. 82.||||||24-NOV-09
12271|Moora Group|24526|5|Briefly described|p114, p106 Fig. 7|||Includes the Billeringa Subgroup.||||||
12271|Moora Group|24542|6|Mentioned|p2 Fig.2, p11|Proterozoic|Proterozoic|||||||
12271|Moora Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
12271|Moora Group|31051|6|Mentioned|p78|||Re quartzite.||||||
12271|Moora Group|31154|6|Mentioned|p71|||||||||
12271|Moora Group|31393|6|Mentioned|Pl.25|||||||||
12271|Moora Group|31561|6|Mentioned|p3|||||||||
12271|Moora Group|31562|5|Briefly described|p5|||||||||
12271|Moora Group|32644|6|Mentioned|p8|||||||||
12271|Moora Group|33044|6|Mentioned|p32|||See also P40||||||
12271|Moora Group|34287|6|Mentioned|p36|||||||||
12271|Moora Group|34413|6|Mentioned|p12|||||||||
12271|Moora Group|34414|6|Mentioned|p52|||||||||
12271|Moora Group|34705|6|Mentioned|p398|||||||||
12271|Moora Group|36293|2|Defined|p61|Neoproterozoic|Mesoproterozoic|Middle or Late Proterozoic.||||||
12271|Moora Group|36551|6|Mentioned|p141|||||||||
12271|Moora Group|36872|3|Fully described|p75|||||||||
12271|Moora Group|37299|6|Mentioned|Fig.1|||||||||
12271|Moora Group|37344|6|Mentioned|p74|||||||||
12271|Moora Group|37460|4|Described|p178|||||||||
12271|Moora Group|37915|6|Mentioned|p461|||||||||
12271|Moora Group|38243|6|Mentioned|Fig.2|||||||||
12271|Moora Group|38769|6|Mentioned|p79|||||||||
12271|Moora Group|38988|6|Mentioned|p13|||||||||
12271|Moora Group|40105|6|Mentioned|p307|||||||||
12271|Moora Group|40307|6|Mentioned|p62|||||||||
12271|Moora Group|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12271|Moora Group|40347|4|Described|p16|||||||||
12271|Moora Group|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
12271|Moora Group|40349|4|Described|p13|||||||||
12271|Moora Group|40900|6|Mentioned|p34|||||||||
12271|Moora Group|41271|6|Mentioned|p228|||||||||
12271|Moora Group|41341|6|Mentioned|p8|||||||||
12271|Moora Group|41957|6|Mentioned|p68|||||||||
12271|Moora Group|42038|6|Mentioned|p108|||||||||
12271|Moora Group|43096|6|Mentioned|p3|||||||||
12271|Moora Group|43495|6|Mentioned|5|||||||||
12271|Moora Group|44138|5|Briefly described|p264 Fig.3-54, p265, p272||||||Billeranga Subgroup, Coomberdale Subgroup|||
12271|Moora Group|44144|6|Mentioned|p495, p522|Proterozoic|Proterozoic|Excluded from Perth Basin in this article; a component of Pinjarra Orogen.||||||
12271|Moora Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
12271|Moora Group|45965|14|Not recorded|p.58|||||||||
12271|Moora Group|60556|5|Briefly described|p2 Fig. 2, p3|Proterozoic||||||||
12271|Moora 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.||||||
12271|Moora Group|62381|6|Mentioned|p2 Fig.2.|||||||||
12271|Moora Group|63866|6|Mentioned|p183|||||||||
12271|Moora Group|64580|4|Described|map legend||Mesoproterozoic|Sandstone, siltstone, dolostone, stromatolitic dolostone and silicified dolostone; basalt and volcanic sandstone.||||||09-DEC-08
12271|Moora Group|64635|6|Mentioned|p2 Fig.1, p5 Fig.4|||||||||
12271|Moora Group|64722|5|Briefly described|Fig. 2 p3-6, p20|Ectasian|Calymmian|Adjacent to the Darling Fault. Age from Rb-Sr dating in lower part of Group.|1390 +/- 140 Ma.||||Predominantly siliciclastic strata with some volcanic and volcaniclastic rocks and minor dolomite.|11-APR-12
12271|Moora Group|64769|6|Mentioned|p117|Proterozoic|Proterozoic|WA. Sedimentary rocks.||||||06-MAY-09
12271|Moora Group|65487|6|Mentioned|p2 Fig.1|||||||||
12271|Moora Group|67340|6|Mentioned|p7-8, 25, 35, 55|Proterozoic|Proterozoic|Basement to north Perth Basin. Thermal rock properties.||||||
12271|Moora Group|69003|6|Mentioned|vi, p28, p54, p72|||||||||
12271|Moora Group|69182|6|Mentioned|Ch2 p3|||Perth Basin.||||||
12271|Moora Group|69558|6|Mentioned|p177|Proterozoic|Proterozoic|||||||
12271|Moora Group|69583|6|Mentioned|p132|||Pinjarra Orogen.||||||
12271|Moora Group|69595|6|Mentioned|p3 fig 1|||||||||
12271|Moora Group|70090|6|Mentioned|p442|||Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin.||||||
12271|Moora Group|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Neoproterozoic|Moora Basin, Pinjarra Orogen. Affected by the Leeuwin Orogeny . See also 2_5m_interpgeop15_lut.csv.|ca. 1000  531 Ma (inferred)||Includes the Coomberdale Subgroup and the Billeranga Subgroup.||Sandstone, siltstone; basalt (in lower part), and dolomite and silicified dolomite (in upper part).|
12271|Moora Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Moora Basin.||||||20-APR-20
12271|Moora Group|71146|6|Mentioned|p16|Precambrian|Precambrian|Pinjarra Orogen.||||||
12271|Moora Group|71269|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Mesoproterozoic|Geological province: Pinjarra Orogen. Of Moora Basin. Events: Leeuwin Orogeny (780-515 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|1600-541 Ma (inferred)||Includes Billeranga Subgroup, Coomberdale Subgroup.||Sandstone, siltstone; basalt (in lower part), and dolomite and silicified dolomite (in upper part)|
12271|Moora Group|71781|4|Described|p55, Plates 3, 4||||||Includes Coomberdale Chert.|||
12271|Moora Group|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Mesoproterozoic|Moora Basin.|||Includes Coomberdale Subgroup, Billeranga Subgroup.||Sandstone, siltstone; basalt (in lower part), and dolomite and silicified dolomite (in upper part).|
12284|Moorhead Formation|14227|5|Briefly described|Enclos. 2|Early Permian|Early Permian|Of the Stockton Group. Underlies Westralia Sandstone; overlies Shotts Formation. Presented as Moorhead only.||||||07-FEB-11
12284|Moorhead Formation|22820|6|Mentioned|p10 Fig. 4, p13|Early Permian|Early Permian|Of the Stockton Group. Previously mapped as the siltstone section of the former Stockton Formation. Geol.prov: Collie Basin.||||||12-AUG-08
12284|Moorhead Formation|23174|5|Briefly described|Fig5p8|Early Permian|Early Permian|||||||
12284|Moorhead Formation|23279|6|Mentioned|p13|||(Le Blanc Smith, 1993).||||||
12284|Moorhead Formation|42711|2|Defined|p5 Fig. 4, Plates 2, 4|Early Permian|Early Permian|Of Stockton Group. Unconformable on Shotts Fm; conformable below Westralia Sandstone. Max. thickness: 230m. Geol.prov:Collie Basin. Lam'd claystone+subordinate thin beds of buff-coloured siltstone, fine-gr.sandstone+rare limestone lenses.||||||11-AUG-08
12284|Moorhead Formation|43442|6|Mentioned|p50|||||||||
12284|Moorhead Formation|70097|5|Briefly described|p19 Fig.3|Sakmarian|Asselian|Collie Sub-basin.||Stockton Group.||Overlies Shotts Formation. Is overlain by Westralia Sandstone.||
12315|Morawa Lavas|24160|6|Mentioned|p27 Tb. 14|Proterozoic|Proterozoic|||Billeranga Subgroup||||
12315|Morawa Lavas|24522|6|Mentioned|p84, p85|||Age: 1.36-1.32Ga.  Geological Province: Yilgarn Craton.||||||
12315|Morawa Lavas|36293|6|Mentioned|p76|||Refers Arriens & Lalor 1959 and Low 1975.||||||
12315|Morawa Lavas|36872|3|Fully described|p74|||||||||
12315|Morawa Lavas|37460|6|Mentioned|p178|||||||||
12315|Morawa Lavas|40307|6|Mentioned|p62|||||||||
12315|Morawa Lavas|41271|6|Mentioned|p228|||||||||
12315|Morawa Lavas|44144|6|Mentioned|p511|||Rocks of this unit occur as glacial erratics in Nangetty Formation.||||||
12315|Morawa Lavas|67026|6|Mentioned|p344.|||||||||
12315|Morawa Lavas|69003|6|Mentioned|p48 Fig.57|Mesoproterozoic|Mesoproterozoic|Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|c.1360 Ma.|||||
12315|Morawa Lavas|69412|6|Mentioned|p2|||"Yilgarn Craton. Described as ""poorly understood"". May be the first (?only) large layered intrusion or volcanic rocks in the Marnda Moorn LIP."||||||
12315|Morawa Lavas|71169|6|Mentioned|p82|Ectasian|Ectasian|Yilgarn Craton.|c. 1360 Ma|||||
12323|Morelands Group|37373|5|Briefly described|Table 2.I|||||||||
12323|Morelands Group|39869|6|Mentioned|Fig.2|||||||||
12323|Morelands Group|41249|5|Briefly described|Table 1|||||||||
12323|Morelands Group|43075|5|Briefly described|Table 1|||||||||
12360|Mortigup Granodiorite|38513|6|Mentioned|Table IV|||||||||
12360|Mortigup Granodiorite|38789|6|Mentioned|Table 2|||||||||
12360|Mortigup Granodiorite|40775|4|Described|p500|||||||||
12362|Mortimer Hills Pegmatite|40303|6|Mentioned|p28|||||||||
12410|Mosquito Creek Formation|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3000Ma.||||||07-NOV-08
12410|Mosquito Creek Formation|22717|6|Mentioned|P5|||||||||
12410|Mosquito Creek Formation|23255|6|Mentioned|Fig.2|||||||||
12410|Mosquito Creek Formation|23755|6|Mentioned|p6|||Of De Grey Group. Geological Province: Pilbara Craton.||||||
12410|Mosquito Creek Formation|23784|5|Briefly described|p6|Archean|Archean|Of de Grey Group.||||||07-NOV-08
12410|Mosquito Creek Formation|23793|6|Mentioned|p6|||Geological Province: Pilbara Craton||||||
12410|Mosquito Creek Formation|23813|5|Briefly described|p104|Archean|Archean|Max. thickness: 5000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|23936|5|Briefly described|p3, p19, Fig.19a|Archean|Archean|Geological Province: Pilbara Craton. Underlying Unit: Warrawoona Group (unconformably).||||||07-NOV-08
12410|Mosquito Creek Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: >5000m.  Psammitic, psammopelitic and pelitic rocks with minor conglomerate.  Geological Province: Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: De Grey Group.  Geological Province: Pilbara Craton||||||07-NOV-08
12410|Mosquito Creek Formation|24184|5|Briefly described|p717|Archean|Archean|Geological Province: Pilbara Craton. Max age:3312Ma||||||07-NOV-08
12410|Mosquito Creek Formation|24185|5|Briefly described|p742 Tb.4, p748|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|24188|4|Described|p789, 795|Archean|Archean|Age: <3000 Ma. Interpreted to be pair of the <3000 Ma De Grey Groups; also Krapez (1993) 3240 Ma. Geological Province: Pilbara Craton||||||07-NOV-08
12410|Mosquito Creek Formation|31310|6|Mentioned|p54|||||||||
12410|Mosquito Creek Formation|31311|6|Mentioned|p67|||||||||
12410|Mosquito Creek Formation|31853|6|Mentioned|p60|||Refers Hickman (in prep.)||||||
12410|Mosquito Creek Formation|35269|6|Mentioned|p297|||||||||
12410|Mosquito Creek Formation|35726|6|Mentioned|p36|||||||||
12410|Mosquito Creek Formation|35978|6|Mentioned|p118|||||||||
12410|Mosquito Creek Formation|36551|6|Mentioned|p42|||||||||
12410|Mosquito Creek Formation|38498|5|Briefly described|Table 1|||||||||
12410|Mosquito Creek Formation|38544|6|Mentioned|Fig.1|||||||||
12410|Mosquito Creek Formation|38763|6|Mentioned|p108|||||||||
12410|Mosquito Creek Formation|39424|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
12410|Mosquito Creek Formation|39426|2|Defined|Table 1|Archean|Archean|||||||07-NOV-08
12410|Mosquito Creek Formation|39672|6|Mentioned|Fig.1|||||||||
12410|Mosquito Creek Formation|39697|3|Fully described|p102|||See also p19.||||||21-AUG-07
12410|Mosquito Creek Formation|41066|5|Briefly described|1 of 2 K01|||||||||
12410|Mosquito Creek Formation|41252|6|Mentioned|p49|||||||||
12410|Mosquito Creek Formation|41357|5|Briefly described|p129|||||||||
12410|Mosquito Creek Formation|41561|5|Briefly described|p535|||||||||
12410|Mosquito Creek Formation|41635|5|Briefly described|p21|||||||||
12410|Mosquito Creek Formation|41669|5|Briefly described|p10|||||||||
12410|Mosquito Creek Formation|42231|6|Mentioned|Table 1 P330|||||||||
12410|Mosquito Creek Formation|42730|6|Mentioned|p7|||||||||
12410|Mosquito Creek Formation|43055|5|Briefly described|p8|||||||||
12410|Mosquito Creek Formation|43056|5|Briefly described|Map Legend|||of Gorge Creek Group||||||
12410|Mosquito Creek Formation|43595|5|Briefly described|p213|||||||||
12410|Mosquito Creek Formation|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p135|||See also p152 Tb.2-22, p155, p157 Fig.2-144. Over 5km thick in places. In West Pilbara contains granitoid clasts but in East the clasts indicate reworking of Warrawoona Group (volcanics, chert, BIF pebbles etc).||Gorge Creek Group||Unconformably overlies Warrawoona Group. Overlain unconformably by Fortescue Group.|Schistose, psammitic and pelitic metasedimentary rocks (poorly sorted siltstone and sandstone, intercalated with pelites), with subordinate conglomerate.|
12410|Mosquito Creek Formation|44151|5|Briefly described|p163|||Complex structural history.||Gorge Creek Group.|||Metamorphosed quartz-feldspar wacke, metasiltstone, quartz-mica schist, and quartzite.|
12410|Mosquito Creek Formation|44152|6|Mentioned|p170|||Source for Beatons Creek Conglomerate at Nullagine.||Gorge Creek Group||||
12410|Mosquito Creek Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group (Pilbara Supergroup). Geological Province: Mosquito Creek Basin, Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|50435|5|Briefly described|p2.1, 2.3|Archean|Archean|Geological Province: Kimberley Block. Age: ~3000Ma. Intruded by Bridget Suite.||||||07-NOV-08
12410|Mosquito Creek Formation|60429|6|Mentioned|p18|||Originally of the Gorge Creek Group, now reassigned to De Grey Group.||||||07-FEB-11
12410|Mosquito Creek Formation|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|Of the Nullagine Group. Geological Province: eastern Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|61264|4|Described|p62-68|Archean|Archean|Of the Nullagine Group (De Grey Supergroup). Succession of siliciclastic rocks. Conformably overlies Coondamar Formation.  Age: 2926-2905Ma. Geological Province: Mosquito Creek/Pilbara Craton.||||||07-NOV-08
12410|Mosquito Creek Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Nullagine Group (De Grey Supergroup). Geological Province: Pilbara Craton. Metamorphosed sandstone, siltstone and shale; graded bedding and local cross-bedding; includes metamorphosed turbidite deposits.||||||07-NOV-08
12410|Mosquito Creek Formation|63441|4|Described|p5 Tb.1, p29-30|Archean|Archean|Of Nullagine Group (De Grey  Supergp).Conformable on Coondamar Fm.Max.age:2926+/-29Ma. Est.at ~5km thick. Lower part: interbedded conglom., massive coarse-gr. sst, siltst.+shale: upper part: thinly bedded sst interbedded with siltst.+ shale; metamorphosed||||||07-FEB-11
12410|Mosquito Creek Formation|63538|4|Described|p7, p6 Fig. 3|Archean|Archean|Overlies Coondamar Formation. Age: c. 2926Ma. Geological Province: Pilbara Craton. Fine- to coarse-grained siliciclastic sedimentary rocks.||||||19-APR-13
12410|Mosquito Creek Formation|63854|4|Described|p228-242.|Mesoarchean|Mesoarchean|Central Mosquito Creek Basin, northern Pilbara Craton. Multiply deformed and sub-greenschist to greenschist facies. Hosts epizonal to mesozonal orogenic Au(-Sb) deposits giving minimum age (Pb-Pb model ages on epigenetic galena; I.R. Fletcher, quoted in Thorpe et al.,1992). Maximum age from detrital zircons (Bagas et al. 2008). Geochemistry detailed and provenance discussed.|Between 2972 +14/-37 Ma and 2905 +/- 9 Ma.|Of the Nullagine Group.||Conformably overlies the Coondamar Formation. Is overlain unconformably by Fortescue Group.|Succession of interbedded conglomerate, coarse-grained sandstone, siltstone and shale.|
12410|Mosquito Creek Formation|63866|5|Briefly described|p144|||||||Intruded by the Bridget Suite.||
12410|Mosquito Creek Formation|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness: >5km.||||||07-FEB-11
12410|Mosquito Creek Formation|64580|4|Described|map legend||Mesoarchean|Of Nullagine Group. Metamorphosed sandstone, siltstone, and shale; graded bedding and local cross-bedding; includes metamorphosed turbidite deposits.||||||09-DEC-08
12410|Mosquito Creek Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of De Grey Group. Geological Province: Pilbara Craton. Fine- to medium-grained wacke, siltstone and shale; commonly with graded bedding, rare cross-bedding, probable turbidite deposits; metamorphosed.||||||07-FEB-11
12410|Mosquito Creek Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Nullagine Group. Age: 2926-2905Ma. Geological Province: Pilbara Craton. Metamorphosed sandstone, siltstone, and shale; graded bedding, and local cross-bedding; includes metamorphosed turbidite deposits.||||||26-NOV-08
12410|Mosquito Creek Formation|65008|4|Described|p2, p7, p8, p15-19, p21-25, p27-29, p41|Mesoarchean|Mesoarchean|Mosquito Creek Basin. Geochronology by: D.R Nelson, in prep., GSWA Record 2004/2. Has a proposed thickness of around 5km (Hickman 1983). Hosts significant lode Au and Au-Sb deposits.|ca. 2926 Ma|Of the De Grey Group||Unconformably overlain by the Black Range Dolerite suite?, Copper Gorge Formation?, and Fortescue Group. Overlain by the Beaton Creek Member. Intruded by the Bridget Suite.|Well cleaved and tightly folded interbedded conglomerate and coarse-grained sandstone, with interbedded sandstone, siltstone, and shale displaying graded bedding.|
12410|Mosquito Creek Formation|65825|3|Fully described|p1, p4, p6, pp14-15, pp19-20. |Archean|Archean|Mosquito Creek Basin. An upper, turbidite succession. In the northeast margin of the Basin, unconformably overlies the East Pilbara Granite-Greenstone Terrane. Appendix 2 shows this as a unit in the Nullagine Group of the De Grey Supergroup, according to the GSWA databases. As defined by Hickman (1978), includes the Coondamar Formation; now separated on the bases of new geochronological data and field mapping. Mapped as five separate but un-named sub-units based on differing lithologies, each of which is described in this report. Multiply foliated and metamorphosed under very low to low-grade conditions. Isolated outcrops of ferruginous duricrust cap this unit in the north. Hosts Eastern Creek and Mosquito Creek gold mining centres.|c.2926 - 2905 Ma (Bagas et al. 2004b).|Unit in De Grey Group.||Paraconformably overlies Coondamar Formation. Is intruded by Bridget Suite monzogranites.|A monotonous sequence of metamorphosed sandtone, siltstone and shale with well-preserved graded bedding; locally abundant ferruginous nodules after (?)pyrite; metashale has extremely fine graphite; pebble conglomerate lenses.|
12410|Mosquito Creek Formation|65827|6|Mentioned|p42|||Intruded by Bridget Suite.||||||21-JAN-22
12410|Mosquito Creek Formation|65828|5|Briefly described|Map legend|Archean|Archean||2926-2905 Ma (Bagas et al. 2004).|Unit in De Grey Group.|||Thin- to medium-bedded sandstone, siltstone and shale; commonly with graded bedding, rare cross-bedding; probable turbidity deposits; metamorphosed. Metamorphosed pebble conglomerate, locally channelised, siliceous siltstone and shale.|
12410|Mosquito Creek Formation|66217|5|Briefly described|p40.|Mesoarchean|Mesoarchean|Mosquito Creek Basin. Age from detrital zircons. Deformed at c.2905 Ma.|<2930 Ma (Bagas et al. 2004).|||Overlies Coondamar Formation.|Entirely siliciclastic succession including turbidites.|
12410|Mosquito Creek Formation|66745|6|Mentioned|p50 Fig.1.|Mesoarchean|Mesoarchean|||Unit in De Grey Supergroup.||||
12410|Mosquito Creek Formation|67201|4|Described|p8, p12 Tb.1, p20, p23|||In northwestern Pilbara Craton, unconformably overlies West Pilbara Superterrane and East Pilbara Terrane. De Grey Superbasin, Mosquito Creek Basin. Old detrital zircons: 3714 Ma (Nelson 2005). Defined by Hickman (1978, 1983). Farrell (2006) divided the Mosquito Basin into Coondamar and Mosquito Formations.|2970-2930 Ma, geochron Bagas et al. 2008|Nullagine Group|||Predominantly clastic sedimentation.|24-NOV-16
12410|Mosquito Creek Formation|68035|5|Briefly described|p291, 293, p286 Fig 3|Mesoarchean|Mesoarchean|Mosquito Creek Basin, De Grey Superbasin. Thickness estimates for the complexely folded unit range between 1 and 5 km, and the maximum age of deposition is approximately 2.98 Ga (Nelson, 2004). Basin originated at c. 3.2 Ga as an ENE-WSW-trending rift between the East Pilbara and Kurrana terranes.|2.93 Ga. Max deposition 2980 Ma.|||Northern and southern margins of the basin are in contact with 3.20 - 3.16 Ga intrusive units (Mount Billroth Supersuite and Dalton Suite).||
12410|Mosquito Creek Formation|68280|6|Mentioned|p3|Mesoarchean|Mesoarchean||2970-2930 Ma|||||
12410|Mosquito Creek Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|Intruded by unnamed monzodiorite and granitoid phases. Age derived from sample of silicified quartz metasandstones (169199.1.pdf, 169200.1.pdf) and constrains the maximum age for deposition of sandstone protoliths.|3290 +/- 11 Ma -2948 +/- 24 Ma (SHRIMP)|Nullagine Group|||Interlayered psammite and pelite; graded bedding and local cross bedding preserved; includes metamorphosed turbidite deposits. Siliceous siltstone and shale; sandstone- massive or cross bedded. Pebble conglomerate.|
12410|Mosquito Creek Formation|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.||Unit of Nullagine Group.|||Metamorphosed sandstone, siltstone, and shale; graded bedding and local cross-bedding; includes metamorphosed turbidite deposits|
12410|Mosquito Creek Formation|69301|4|Described|p9 Tb.1, p16, p20 Tb.2|||Pilbara Craton. Mosquito Creek Basin. Thick: at least 2000 m.|2930 Ma|Nullagine Group||Overlies Coondamar Formation.|Consists of basal sandstones and conglomerates, metamorphosed mid-fan and lower-fan sandstones, siltstones, and shales displaying graded bedding, cross-bedding, sole marks, and Bouma sequences.|
12410|Mosquito Creek 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 169187 (lithic-quartz sandstone) yielded an interpreted maximum depositional age of 3039+\-18 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 169194 (lithic-quartz sandstone) yielded an interpreted maximum depositional age of 3003+\-9 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 169199 (lithic-quartz sandstone) yielded an interpreted maximum depositional age of 3290+\-11 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 169200 (lithic-quartz sandstone) yielded an interpreted maximum depositional age of 2948+\-24 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 177131 (metasandstone) yielded an interpreted maximum depositional age of 2981+\-49 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 178010 (lithic-quartz sandstone) yielded an interpreted maximum depositional age of 3294+\-14 Ma for the sandstone (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv.|2980-2930 Ma (inferred)|Unit of Nullagine Group.|||Massive or cross-bedded sandstone; metamorphosed, siliceous siltstone and shale, pebble and minor cobble conglomerate; interlayered psammite and pelite.|
12410|Mosquito Creek Formation|70022|6|Mentioned|p116|||Mosquito Creek Basin, Pilbara Craton.|2.98-2-93 Ga.|Nullagine Group.|||Lithic quartz sandstone and metasandstone.|
12410|Mosquito Creek Formation|70775|5|Briefly described|p38|||Mosquito Creek Basin. This formation is lithologically similar to the Croydon Group of the Mallina Basin and detrital zircons indicate it is also of a similar age.||||||
12410|Mosquito Creek Formation|71169|5|Briefly described|p63|Mesoarchean|Mesoarchean|Pilbara Craton.|2972-2905 Ma|||||
12410|Mosquito Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, turbidite, sandstone|
12410|Mosquito Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mosquito Creek Basin.||Nullagine Group|||Interlayered psammite and pelite; graded bedding and local cross-bedding preserved; includes metamorphosed turbidite deposits.|
12410|Mosquito Creek Formation|72668|5|Briefly described|p4, p15, p22|||Kurrana Terrane. South eastern Pilbara Craton. Penetrative deformation, granite intrusion and shear-hosted Au mineralization occurred at c. 2905 +/- 9 Ma (Pb-Pb). Contains detritus from the East Pilbara.|c. <2926 Ma|Nullagine Group.||Overlies the Coondamar Formation.|Fine to coarse-grained siliciclastic sedimentary rocks.|13-JAN-22
12436|Mount Abbott lamproite|41158|6|Mentioned|p9|||||||||
12457|Mount Amy Granite|22741|6|Mentioned|P20|||||||||
12457|Mount Amy 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
12457|Mount Amy Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12457|Mount Amy Granite|30533|5|Briefly described|p14|||On Table 1||||||
12457|Mount Amy Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12457|Mount Amy Granite|30896|4|Described|p18|||Adelaidean||||||
12457|Mount Amy Granite|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
12457|Mount Amy Granite|32728|6|Mentioned|Table 4|||||||||
12457|Mount Amy Granite|36885|4|Described|p174|||||||||
12457|Mount Amy Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
12457|Mount Amy Granite|42811|5|Briefly described|p9|||||||||
12457|Mount Amy Granite|43281|5|Briefly described|Map legend||Proterozoic|||||||
12457|Mount Amy Granite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex||Intrudes Lennard Granite and Dyasons Granite.|Grey, non-porphyritic, medium- to fine-grained biotite granite, commonly aplitic and muscovite bearing.|
12457|Mount Amy Granite|48931|3|Fully described|p43|||||||||
12457|Mount Amy Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
12457|Mount Amy Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Paperbark Supersuite|||Foliated biotite-muscovite metasyenogranite; weakly porphyritic|03-AUG-15
12457|Mount Amy Granite|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 biotite--muscovite metasyenogranite; weakly porphyritic|
12457|Mount Amy Granite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.||Unit in Paperbark Supersuite.|||Foliated biotite-muscovite metasyenogranite; weakly porphyritic.|
12457|Mount Amy Granite|70154|5|Briefly described|250k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 250k_interpgeop_lut.csv.|1852-1864 Ma||||Foliated biotite--muscovite metasyenogranite; weakly porphyritic|
12457|Mount Amy 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, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 1m_interpgeop_lut.csv.|1864-1852Ma (inferred)|Unit of Paperbark Supersuite.|||Foliated weakly porphyritic leucocratic biotite muscovite syenogranite, aplite, pegmatite|
12459|Mount Andrew Migmatite|30011|5|Briefly described|p164|||||||||
12459|Mount Andrew Migmatite|30974|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12459|Mount Andrew Migmatite|30976|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12459|Mount Andrew Migmatite|36876|4|Described|p96|||||||||
12459|Mount Andrew Migmatite|37460|6|Mentioned|p181|||||||||
12507|Mount Behn Conglomerate|42860|6|Mentioned|Fig.1|||Variation on Behn Conglomerate.||||||
12507|Mount Behn Conglomerate|43666|6|Mentioned|p24||Famennian|||||||
12546|Mount Bruce Supergroup|22475|6|Mentioned|Fig.1|||||||||
12546|Mount Bruce Supergroup|22689|5|Briefly described|137|||Geol province Hamersley Basin. Mount as 'Mt' in text||||||
12546|Mount Bruce Supergroup|22837|6|Mentioned|Fig.1 p412|||Spelt Mt Bruce Supergroup||||||
12546|Mount Bruce Supergroup|22953|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|23047|6|Mentioned|34|||In the Hamersley Province.||||||10-FEB-09
12546|Mount Bruce Supergroup|23244|6|Mentioned|Fig.1|||of Pilbara Craton.||||||
12546|Mount Bruce Supergroup|23280|6|Mentioned|Fig1p1085|||||||||
12546|Mount Bruce Supergroup|23325|5|Briefly described|map legend|Precambrian|Precambrian|||||||
12546|Mount Bruce Supergroup|23348|5|Briefly described|218 Fig.1|||||||||
12546|Mount Bruce Supergroup|23354|5|Briefly described|316|Paleoproterozoic|Neoarchean|||||||07-NOV-08
12546|Mount Bruce Supergroup|23416|5|Briefly described|Map Legend|Archean|Archean|Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|23484|5|Briefly described|p25|||Geological Pronvince: Pilbara Craton.||||||
12546|Mount Bruce Supergroup|23536|5|Briefly described|p 427|||Mount spelt "Mt" in text.||||||26-JUL-07
12546|Mount Bruce Supergroup|23570|5|Briefly described|p11|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
12546|Mount Bruce Supergroup|23575|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Pilbara Supergroup. Geological Province Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|23598|5|Briefly described|p3|||Geological Province: Hamersley Basin.||||||
12546|Mount Bruce Supergroup|23612|4|Described|p838|Proterozoic|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|23743|5|Briefly described|p2 Fig 1|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|23745|5|Briefly described|p6 Fig 4|Proterozoic|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|23746|5|Briefly described|p6 Fig 4|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|23755|4|Described|p10|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|23774|5|Briefly described|p733 table 1|||Ashburton Fold Belt.||||||
12546|Mount Bruce Supergroup|23783|5|Briefly described|p1|||Geological Province: Hamersley Basin.||||||
12546|Mount Bruce Supergroup|23784|6|Mentioned|p6|||||||||
12546|Mount Bruce Supergroup|23793|5|Briefly described|p7|Paleozoic|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|23813|6|Mentioned|p89|||Geological Province: Hamersley Province.||||||
12546|Mount Bruce Supergroup|23891|5|Briefly described|p89|Archean|Archean|Mount is Mt. in text. Geological Province: Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|23895|5|Briefly described|p884 Fig.1|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|24023|5|Briefly described|p26|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|24025|5|Briefly described|p6|Paleoproterozoic|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|24166|5|Briefly described|p3|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|24182|5|Briefly described|p93 Fig 3.|||Geological Province: Pilbara Craton.  Mount is Mt in text of figure.||||||
12546|Mount Bruce Supergroup|24184|5|Briefly described|p695, p696 Fig.1|Neoarchean|Neoarchean|Geological Province: Hamersley Basin. Age: 2.77-2.40Ga||||||07-NOV-08
12546|Mount Bruce Supergroup|24192|5|Briefly described|p850|Paleoproterozoic|Neoarchean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24193|5|Briefly described|p874, Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|24194|5|Briefly described|p905|Archean|Archean|Age: 2.8-2.6 Ga (Pb isotope). Geological Province: Pilbara Craton||||||07-NOV-08
12546|Mount Bruce Supergroup|24352|5|Briefly described|Map legend|Archean|Archean|Age: 2770-2717Ma.   Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24353|5|Briefly described|p1, p6 Fig.4|Paleoproterozoic|Archean|Age: <2770Ma. Geological Province: Pilbara Craton||||||07-NOV-08
12546|Mount Bruce Supergroup|24391|6|Mentioned|p8-2 Fig.1|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
12546|Mount Bruce Supergroup|24531|5|Briefly described|p7|Paleoproterozoic|Neoarchean|Proposed by Blake and Barley (1992) to rename it the Mount Bruce Megasequence Set.  Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24532|5|Briefly described|Map legend|Archean|Archean|Age: c.2764-2756Ma.||||||07-NOV-08
12546|Mount Bruce Supergroup|24533|5|Briefly described|p4, 10 Fig. 4|Paleoproterozoic|Neoarchean|A cover sequence of dominantly basaltic and sedimentary rocks of very low metamorphic grade unconformably overlying the granite-greenstone terranes. Max. thickness: 10km. Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24534|5|Briefly described|Map legend|Archean|Archean|Age: c.2770-2595Ma.||||||07-NOV-08
12546|Mount Bruce Supergroup|24541|5|Briefly described|p9, p12, p47|||Geological Province: Hamersley Basin. Maximum Thickness: 10km. On Dampier - Barrow Island unconformably overlies the West Pilbara Granite-Greenstone Terrane.||||||
12546|Mount Bruce Supergroup|24543|5|Briefly described|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|24544|4|Described|p6, 54|Paleoproterozoic|Archean|Age: 2770-2430 Ma. Unconformably overlain by Wyloo Group. Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|24554|4|Described|p4|Paleoproterozoic|Neoarchean|Age: c. 2770-2300 Ma. Unconformably overlies the granite-greenstone terranes of the Pilbara Craton. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|24573|6|Mentioned|p670 Fig.1|||Mount is spelt Mt. in text. Geological Province: Pilbara Craton||||||
12546|Mount Bruce Supergroup|24590|5|Briefly described|p20, p26|Early Proterozoic|Neoarchean|Age: ca2.77-2.41Ga. Geological Province: Hamersley Basin.  Mount is Mt in text.||||||07-FEB-11
12546|Mount Bruce Supergroup|29629|6|Mentioned|p899|||||||||
12546|Mount Bruce Supergroup|29663|6|Mentioned|p52|||||||||
12546|Mount Bruce Supergroup|29716|4|Described|Table 1|||||||||
12546|Mount Bruce Supergroup|30482|6|Mentioned|p170|||||||||
12546|Mount Bruce Supergroup|30490|6|Mentioned|p108|||||||||
12546|Mount Bruce Supergroup|30766|6|Mentioned|p7|||||||||
12546|Mount Bruce Supergroup|31034|6|Mentioned|p139|||Refers Thomson et al.||||||
12546|Mount Bruce Supergroup|31392|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|31670|6|Mentioned|p911|||||||||
12546|Mount Bruce Supergroup|31671|6|Mentioned|p9|||||||||
12546|Mount Bruce Supergroup|31815|6|Mentioned|p96|||?equiv. Robinson Range Beds. See also P101||||||
12546|Mount Bruce Supergroup|31819|6|Mentioned|p80|||||||||
12546|Mount Bruce Supergroup|31828|6|Mentioned|p40|||Stratigraphic table||||||
12546|Mount Bruce Supergroup|31940|6|Mentioned|p7|||Equiv. Archaean sediments of Peak Hill Sheet.||||||
12546|Mount Bruce Supergroup|32586|6|Mentioned|p1.48|||||||||
12546|Mount Bruce Supergroup|32817|6|Mentioned|p468|||||||||
12546|Mount Bruce Supergroup|33468|6|Mentioned|p201|||Correlated with Cleve Matamorphics||||||
12546|Mount Bruce Supergroup|33470|6|Mentioned|p461|||||||||
12546|Mount Bruce Supergroup|33472|6|Mentioned|p470|||||||||
12546|Mount Bruce Supergroup|33538|6|Mentioned|Fig.1|||||||||
12546|Mount Bruce Supergroup|33540|6|Mentioned|Fig.2|||||||||
12546|Mount Bruce Supergroup|33542|6|Mentioned|p411|||||||||
12546|Mount Bruce Supergroup|33543|4|Described|p132|||||||||
12546|Mount Bruce Supergroup|33544|5|Briefly described|p30|||L. Prot.||||||
12546|Mount Bruce Supergroup|33545|5|Briefly described|p112|||||||||
12546|Mount Bruce Supergroup|33630|6|Mentioned|p908|||||||||
12546|Mount Bruce Supergroup|33727|6|Mentioned|p36|||||||||
12546|Mount Bruce Supergroup|34066|5|Briefly described|p4|||L.Prot.||||||
12546|Mount Bruce Supergroup|34115|6|Mentioned|p383|||2250-2200 my||||||
12546|Mount Bruce Supergroup|34124|5|Briefly described|Table 1|||||||||
12546|Mount Bruce Supergroup|34135|4|Described|Table 1|||Lower Proterozoic. See also Table 2, PP7,13.||||||
12546|Mount Bruce Supergroup|35078|6|Mentioned|p257|||||||||
12546|Mount Bruce Supergroup|35084|6|Mentioned|p288|||||||||
12546|Mount Bruce Supergroup|35218|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|35255|6|Mentioned|p7|||||||||
12546|Mount Bruce Supergroup|35260|6|Mentioned|p5|||Map legend.||||||
12546|Mount Bruce Supergroup|35269|6|Mentioned|p301|||||||||
12546|Mount Bruce Supergroup|35495|6|Mentioned|p339|||||||||
12546|Mount Bruce Supergroup|35976|1|Redefined|p107|Proterozoic|Proterozoic|||||||
12546|Mount Bruce Supergroup|36003|5|Briefly described|p1025|||||||||
12546|Mount Bruce Supergroup|36004|6|Mentioned|p1089|||||||||
12546|Mount Bruce Supergroup|36247|6|Mentioned|p186|||See also Fig.1.||||||
12546|Mount Bruce Supergroup|36308|6|Mentioned|p200|||||||||
12546|Mount Bruce Supergroup|36551|6|Mentioned|p87|||||||||
12546|Mount Bruce Supergroup|36642|6|Mentioned|Table 1|||||||||
12546|Mount Bruce Supergroup|36870|6|Mentioned|p60|||||||||
12546|Mount Bruce Supergroup|36880|6|Mentioned|p108|||||||||
12546|Mount Bruce Supergroup|36882|3|Fully described|p124|||||||||
12546|Mount Bruce Supergroup|36883|6|Mentioned|p144|||||||||
12546|Mount Bruce Supergroup|36891|6|Mentioned|p442|||||||||
12546|Mount Bruce Supergroup|37297|6|Mentioned|p93|||||||||
12546|Mount Bruce Supergroup|37299|6|Mentioned|Fig.1|||||||||
12546|Mount Bruce Supergroup|37327|6|Mentioned|p389|||||||||
12546|Mount Bruce Supergroup|37373|6|Mentioned|p35|||||||||
12546|Mount Bruce Supergroup|37460|4|Described|p111|||||||||
12546|Mount Bruce Supergroup|37577|6|Mentioned|p6|||||||||
12546|Mount Bruce Supergroup|37633|6|Mentioned|Plate 1|||||||||
12546|Mount Bruce Supergroup|37708|6|Mentioned|Fig.2|||||||||
12546|Mount Bruce Supergroup|37934|6|Mentioned|p555|||||||||
12546|Mount Bruce Supergroup|38243|6|Mentioned|p353|||||||||
12546|Mount Bruce Supergroup|38326|6|Mentioned|p342|||||||||
12546|Mount Bruce Supergroup|39200|6|Mentioned|p273|||||||||
12546|Mount Bruce Supergroup|39210|3|Fully described|p41|||See also Table 1.||||||24-JUL-07
12546|Mount Bruce Supergroup|39558|6|Mentioned|Table 1|||||||||
12546|Mount Bruce Supergroup|39672|5|Briefly described|Fig.2|||||||||
12546|Mount Bruce Supergroup|39697|6|Mentioned|Table 2|||||||||
12546|Mount Bruce Supergroup|39837|6|Mentioned|p257|||||||||
12546|Mount Bruce Supergroup|39952|5|Briefly described|p289|||||||||
12546|Mount Bruce Supergroup|40089|6|Mentioned|p4|||||||||
12546|Mount Bruce Supergroup|40103|6|Mentioned|Fig.1|||||||||
12546|Mount Bruce Supergroup|40369|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|40839|6|Mentioned|p229|||||||||
12546|Mount Bruce Supergroup|40852|6|Mentioned|p22|||||||||
12546|Mount Bruce Supergroup|40937|5|Briefly described|p2|||||||||
12546|Mount Bruce Supergroup|40938|6|Mentioned|p8|||||||||
12546|Mount Bruce Supergroup|41028|5|Briefly described|p227|||||||||
12546|Mount Bruce Supergroup|41243|6|Mentioned|p258|||||||||
12546|Mount Bruce Supergroup|41252|6|Mentioned|p51|||||||||
12546|Mount Bruce Supergroup|41263|6|Mentioned|p57|||||||||
12546|Mount Bruce Supergroup|41349|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|41357|5|Briefly described|p123|||||||||
12546|Mount Bruce Supergroup|41358|6|Mentioned|p144|||||||||
12546|Mount Bruce Supergroup|41561|5|Briefly described|p535|||||||||
12546|Mount Bruce Supergroup|41843|6|Mentioned|p67|||||||||
12546|Mount Bruce Supergroup|41846|6|Mentioned|p94|||||||||
12546|Mount Bruce Supergroup|41957|5|Briefly described|p67|||||||||
12546|Mount Bruce Supergroup|42020|5|Briefly described|p316|||||||||
12546|Mount Bruce Supergroup|42148|6|Mentioned|p685|||||||||
12546|Mount Bruce Supergroup|42190|5|Briefly described|p273|||See also Fig.3, Fig.4 Map||||||
12546|Mount Bruce Supergroup|42231|6|Mentioned|p336|||||||||
12546|Mount Bruce Supergroup|42260|5|Briefly described|p7|||||||||
12546|Mount Bruce Supergroup|42342|5|Briefly described|p21|||||||||
12546|Mount Bruce Supergroup|42435|6|Mentioned|p46|||||||||
12546|Mount Bruce Supergroup|42471|5|Briefly described|p4|||||||||
12546|Mount Bruce Supergroup|42730|5|Briefly described|p5|||Actually spelt Mt Bruce Supergroup.||||||
12546|Mount Bruce Supergroup|42744|5|Briefly described|p3|||||||||
12546|Mount Bruce Supergroup|42785|5|Briefly described|p261|||see also Fig.2 P263||||||
12546|Mount Bruce Supergroup|42898|5|Briefly described|p339, Fig.2 p341|||actually spelt Mt Bruce Supergroup||||||
12546|Mount Bruce Supergroup|43037|5|Briefly described|Table 1,p24|||||||||
12546|Mount Bruce Supergroup|43056|5|Briefly described|Map Legend|||||||||
12546|Mount Bruce Supergroup|43063|5|Briefly described|Fig.1,p48|||||||||
12546|Mount Bruce Supergroup|43064|6|Mentioned|p65|||||||||
12546|Mount Bruce Supergroup|43119|6|Mentioned|p13|||||||||
12546|Mount Bruce Supergroup|43290|6|Mentioned|p4,p8.||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|43595|4|Described|p75,fig.2-48,p218-9|||||||||
12546|Mount Bruce Supergroup|43769|6|Mentioned|Fig.1,p856|||||||||
12546|Mount Bruce Supergroup|43779|6|Mentioned|p6|||2800 Ma: basal strata age||||||
12546|Mount Bruce Supergroup|43821|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|43822|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|44150|6|Mentioned|p132 Fig.2-131||||||Includes Fortescue Group.|Unconformably overlies Pilbara Supergroup.||
12546|Mount Bruce Supergroup|44152|5|Briefly described|p163-191|Siderian|Neoarchean|Formerly Nullagine Beds or Nullagine Series (Maitland, 1904, 1905, 1906, 1908; Talbot, 1920). Name proposed by MacLeod et al. (1963); revised by Trendall (1979). Hamersley Basin. Up to 10 km thick; outcrop area c.100 000 sq. km.|||Includes Fortescue, Hamersley, Turee Creek Groups.|||
12546|Mount Bruce Supergroup|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|44229|5|Briefly described|Map Legend|Archean|Archean|Includes the Fortescue Group.||||||07-NOV-08
12546|Mount Bruce Supergroup|44477|5|Briefly described|p.7||Proterozoic|SF/50-6.||||||
12546|Mount Bruce Supergroup|44478|14|Not recorded|map legend||Proterozoic|||||||
12546|Mount Bruce Supergroup|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
12546|Mount Bruce Supergroup|44501|14|Not recorded|p.6,10,11, map||Paleoproterozoic|(ref. to Halligan and Daniels 1964). (F/50-7). Lower Proterozoic.||||||07-NOV-08
12546|Mount Bruce Supergroup|44502|14|Not recorded|map legend||Proterozoic|||||||
12546|Mount Bruce Supergroup|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
12546|Mount Bruce Supergroup|44536|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
12546|Mount Bruce Supergroup|44692|4|Described|p.6,9, map|||(F50-11).||||||
12546|Mount Bruce Supergroup|44729|5|Briefly described|map legend|Proterozoic||||||||
12546|Mount Bruce Supergroup|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|50131|6|Mentioned|p3|Early Proterozoic|Archaean|Includes Fortescue, Hamersley and Turee Creek Groups. Volcanic and sedimentary rocks.||||||
12546|Mount Bruce Supergroup|50146|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
12546|Mount Bruce Supergroup|50216|5|Briefly described|p208|Paleoproterozoic|Archean|Includes the Fortescue, Hamersley and Turee Creek Groups. Max. thickness: 10 km.||||||07-NOV-08
12546|Mount Bruce Supergroup|50226|5|Briefly described|p415|||Unconformably overlain by the Wyloo Group.||||||
12546|Mount Bruce Supergroup|50287|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|50300|5|Briefly described|Map Legend|Archean|Archean|Includes: Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|50370|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|50381|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|50423|6|Mentioned|p215 Fig.1||Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|50427|6|Mentioned|p182 Fig.5|Archean|Archean|||||||07-NOV-08
12546|Mount Bruce Supergroup|50435|6|Mentioned|p2.1|||Geological Province: Kimberley Block. Intruded by Bridget Suite.||||||
12546|Mount Bruce Supergroup|50544|4|Described|p42|Neoarchean|Neoarchean|Comprises Fortescue Group, Carawine Dolomite (Hamersley Group).  Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|50549|5|Briefly described|p1158|Paleoproterozoic|Archean|Contains Fortescue Group, Hamersley Group and Turee Creek Group.||||||07-NOV-08
12546|Mount Bruce Supergroup|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Fortescue and Hamersley Groups.  Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|60373|5|Briefly described|p145 Tb. 1|Paleoproterozoic|Archean|Includes; Turee Creek, Hamersley and Fortescue Groups.||||||
12546|Mount Bruce Supergroup|60429|6|Mentioned|p2|||Geological Province: Pilbara Craton.||||||07-FEB-11
12546|Mount Bruce Supergroup|60539|5|Briefly described|p498 Fig.1|Paleoproterozoic|Archean|Includes: Turee Creek Group, Hamersley Group, Fortesque Group. Overlain by Wyloo Group. Geological Province: Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|60636|6|Mentioned|p11|Archean|Archean|Age: ~2.77-2.40Ga.||||||07-FEB-11
12546|Mount Bruce Supergroup|60706|5|Briefly described|p622|||Comprised of the Fortescue, Hamersley and Turee Groups. Mount is Mt in text. Geological Province: Hamersley Basin.||||||
12546|Mount Bruce Supergroup|60903|5|Briefly described|p833 Fig. 2|Archean|Archean|Age: 2.77-2.40Ga.  Geological Province: Pilbara Craton. Mount is Mt in text.||||||07-NOV-08
12546|Mount Bruce Supergroup|61253|6|Mentioned| p51|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|61264|5|Briefly described|p64 Fig. 2|||Includes the Fortescue Group.||||||17-MAY-06
12546|Mount Bruce Supergroup|61268|5|Briefly described|p77|Paleoproterozoic|Archean|Deposited between 2.77 and 2.40 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|61576|5|Briefly described|p773|||Includes the Hamersley Group. Volcanic and sedimentary deposits. Max. thickness: 9km. Geological Province: Pilbara Craton.||||||
12546|Mount Bruce Supergroup|62129|4|Described|p5, p17|Archaean|Archaean|Includes Hamersley, Fortescue and Turee Creek Groups. Geological Province: Hamersley Basin.||||||07-FEB-11
12546|Mount Bruce Supergroup|62130|5|Briefly described|Map Legend|Archaean|Archaean|Includes; Fortescue Group, Hamersley Group and Turee Creek Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||23-MAR-09
12546|Mount Bruce Supergroup|62289|6|Mentioned|p2|||||||||
12546|Mount Bruce Supergroup|62579|5|Briefly described|p116|Archean|Archean|Includes Fortescue, Hamersley and Turee Groups. Mount is Mt in text. Geological Povince: Pilbara Craton.||||||07-NOV-08
12546|Mount Bruce Supergroup|63139|5|Briefly described|p50|Paleoproterozoic|Neoarchean|Includes Fortescue and Hamersley Groups. Unconformably overlies ca 3500Ma  to ca 2850Ma granite-greenstone terrain.||||||07-NOV-08
12546|Mount Bruce Supergroup|63153|5|Briefly described|p1359, p1363 |||Hamersley province.|||Includes Fortescue, Hamersley and Turee Creek Groups.|Is overlain unconformably by Wyloo Group.||
12546|Mount Bruce Supergroup|63367|5|Briefly described|p230, ||||||Includes the Fortescue, Hamersley and Turee Creek Groups.|||
12546|Mount Bruce Supergroup|63372|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|63417|5|Briefly described|Map legend|Archean|Archean|Comprises Fortescue and Hamersley Groups. Age: c.2772-~2548Ma. Geological Province: Fortescue and Hamersley Basins.||||||07-NOV-08
12546|Mount Bruce Supergroup|63420|5|Briefly described|Map legend|Archean|Archean|Includes the Fortescue Group. Age ranges: c.2775Ma, c. 2764-2756Ma and c.2741Ma. Geological Province: Marble Bar Sub-basin/Hamersley Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|63432|5|Briefly described|p735 Fig. 1|||Geological Province: Pilbara Craton.||||||07-FEB-11
12546|Mount Bruce Supergroup|63538|6|Mentioned|p1|||||||||07-FEB-11
12546|Mount Bruce Supergroup|63854|5|Briefly described|p229 Fig.2 ||||||Includes the Fortescue Group.|||
12546|Mount Bruce Supergroup|63866|5|Briefly described|p144, p151, p154|||Hamersley Basin.|||Includes the Beasley River Quartzite, Fortescue, Turee Creek and Hamersley Groups.|Intruded by the Bridget Suite. Unconformably overlain by the Wyloo Group.||
12546|Mount Bruce Supergroup|63869|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic||||Includes Turee Creek Group.|||
12546|Mount Bruce Supergroup|64174|5|Briefly described|Map legend|Archean|Archean|Includes Hamersley and Fortescue Groups. Age: 2775-2629Ma. Geological Province: West Pilbarra Terrane, Gorge Creek Basin, Whim Creek Basin.||||||07-NOV-08
12546|Mount Bruce Supergroup|64326|5|Briefly described|p70|Archean|Archean|Forms and overlying cover succession deposited over the Hamersley Basin from c.2770 to 2400Ma. This comprises Fortescue group (top), Hamersley Group (middle) and Turee Creek Group (basalt0.||||||07-FEB-11
12546|Mount Bruce Supergroup|64384|6|Mentioned|p1, p29|Paleoproterozoic|Archean|Comprises Fortescue, Hamersley and Turee Creek Groups. Geological province: Hamersley Basin.||||||07-FEB-11
12546|Mount Bruce Supergroup|64580|6|Mentioned|map legend|||||||||
12546|Mount Bruce Supergroup|64621|5|Briefly described|Map legend|Archean|Archean|Includes the Fortescue Group.||||||07-NOV-08
12546|Mount Bruce Supergroup|64653|5|Briefly described|Map Legend|Archaean|Archaean|Includes the Fortescue Group. Geological Province: Pilbara Craton.||||||07-FEB-11
12546|Mount Bruce Supergroup|64654|5|Briefly described|Map Legend|Archaean|Archaean|Includes Hamersley  and Fortescue Groups. Age: c. 2766Ma - c. 2597Ma. Geological Province: Pilbara Craton (Hamersley Basin).||||||
12546|Mount Bruce Supergroup|64656|5|Briefly described|Map Legend|Archaean|Archaean|Includes Fortescue Group. Geological Province: Hamersley Basin.||||||
12546|Mount Bruce Supergroup|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Fortescue and Hamersely Groups. Geological Province: Hamersley Basin.||||||
12546|Mount Bruce Supergroup|64728|5|Briefly described|p94 Fig.1, p107.|||Main source of detrital zircons in Wyloo Group.|c.2780-2208 Ma.|||Underlies Wyloo Group.||
12546|Mount Bruce Supergroup|64830|5|Briefly described|p1108|||Contains the Hamersley Group. Geological province: Hamersley Basin.||||||05-FEB-09
12546|Mount Bruce Supergroup|64936|5|Briefly described|map legend|Archean|Archean|Includes Fortescue Group. Geol. Prov: Pilbara Craton.||||||
12546|Mount Bruce Supergroup|65008|5|Briefly described|p5, p7, p8 Fig.5, p41|Archean|Archean|Hamersley Basin.|||Includes the Fortescue Group.|Unconformably underlain by the Pilbara Supergroup.||
12546|Mount Bruce Supergroup|65194|5|Briefly described|p98 Fig.4.23|||Includes Turee Creek, Hamersley and Fortescue Groups.||||||11-APR-16
12546|Mount Bruce Supergroup|65415|6|Mentioned|p118, p120 Fig.2, p121.|||||||Unconformably overlies Mount Negri Volcanics.||
12546|Mount Bruce Supergroup|65683|5|Briefly described|p799|Siderian|Neoarchean|Unconformable lower boundary. 2750-2300 Ma. Includes Fortescue Group, Hamersley Group, Turee Creek Group.||||||08-MAR-12
12546|Mount Bruce Supergroup|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Includes Hamersley Group and Fortescue Group, and constituents. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
12546|Mount Bruce Supergroup|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|||Includes Fortescue Group.|||
12546|Mount Bruce Supergroup|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|||Includes Fortescue Group.|||
12546|Mount Bruce Supergroup|65825|4|Described|p7 Fig.4,  p20. |Archean|Archean|Referred to as Mount Bruce Megasequence by Blake and Barley (1992). Encompasses all the stratigraphic units in the Hamersley Basin overlying the granite-greenstone basement.|||Includes Fortescue Group, Hamersley Group and Pinjian Chert Breccia.||A basal volcano-sedimentary succession and an overlying succession of chert/banded iron-formation/dolomite.|
12546|Mount Bruce Supergroup|65827|6|Mentioned|p2, p42|||Hamersley Basin. Includes Fortescue Group. Intruded by Bridget Suite.||||||21-JAN-22
12546|Mount Bruce Supergroup|65828|6|Mentioned|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|||Includes Fortescue and Hamersley Groups and an un-named unit of dolerite dykes and sills.|||
12546|Mount Bruce Supergroup|65829|6|Mentioned|p4, p14. ||||||Includes Fortescue and Hamersley Groups.|||
12546|Mount Bruce Supergroup|65830|6|Mentioned|p3|||Underlies the Ashburton Basin succession.|||Includes Turee Creek Group.|||
12546|Mount Bruce Supergroup|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin. Shown as comprising Fortescue Group and Black Range Dolerite Suite.||||||
12546|Mount Bruce Supergroup|66115|5|Briefly described|p136|Paleoproterozoic|Neoarchean|||||Is disconformaby overlain by Wyloo Group.|Modestly to moderately metamorphosed iron formations carbonates and other lithologies.|
12546|Mount Bruce Supergroup|66118|4|Described|p146, p153 Fig.7|||Fortescue Basin.|c. 2780-2450 Ma||Fortescue Group|Unconformably overlies Pilbara Craton in the south.|Volcanic and sedimentary rocks.|
12546|Mount Bruce Supergroup|66217|4|Described|p1, p2, p5, p39, pp44-55.|Paleoproterozoic|Neoarchean|Marble Bar Sub-basin; Fortescue Basin, Pilbara Craton. Unconformably overlies Archean (3.65-2.83 Ga) granite and greenstone basement. Affected by at least nine sets of syn-depositional deformation.|2775-2300 Ma.||Includes Fortescue, Hamersley and Turee Creek Groups.|Unconformably overlies De Grey Supergroup. Is intruded by Bridget Suite. Is unconformably overlain by the Wyloo Group.|Volcanic and sedimentary rocks.|
12546|Mount Bruce Supergroup|66574|5|Briefly described|p912, p920 Fig.9|Orosirian|Neoarchean|Contains Fortescue, Hamersley and Turee Creek Groups. Is overlain unconformably by Wyloo Group.||||||
12546|Mount Bruce Supergroup|66685|6|Mentioned|p216|Archean|Archean|Pilbara Craton.|2780-2450 Ma|||||
12546|Mount Bruce Supergroup|66745|5|Briefly described|p50 Fig.1.|Neoarchean|Neoarchean||2780-2450 Ma.||Includes Fortescue and Hamersley Groups.|||
12546|Mount Bruce Supergroup|66882|6|Mentioned|p118|||Pilbara Craton. The unconformably-underlying basement is a possible source for Mesoarchean zircons in Cook Gap Schist (Gawler Craton).||||||
12546|Mount Bruce Supergroup|67025|5|Briefly described|pp318-319, p328.|Paleoproterozoic|Archean|Hamersley Basin, Pilbara Block.|||Includes Fortescue, Hamersley and Turee Creek Groups.|Is overlain unconformably by the Wyloo Group||
12546|Mount Bruce Supergroup|67056|5|Briefly described|p419 Fig.2, p422. |Paleoproterozoic|Archean||||Includes Fortescue, Hamersley and Turee Creek Groups.|Southern margins are overlain unconformably by the Wyloo Group.||
12546|Mount Bruce Supergroup|67130|6|Mentioned|p6||||||Includes Fortescue Group, Hamersley Group, Turee Creek Group|||
12546|Mount Bruce Supergroup|67183|5|Briefly described|p640 Fig.1, p641-2, p649 Fig.8, p651, |Paleoproterozoic|Archean|Represents basin development over a period of 270 Ma. Age of 2760-2490 Ma from Trendall (1983, 1990); Black and McNaughton (1984).|2760-2490 Ma||Hamersley Group, Fortescue Group, Turee Creek Group, Carawine Dolomite|||17-JUL-15
12546|Mount Bruce Supergroup|67201|5|Briefly described|p16-17 Fig.9|Archean|Archean||||Fortescue Group|||
12546|Mount Bruce Supergroup|67229|6|Mentioned|p3|||Pilbara region.|||Fortescue, Hamersley, Turee Creek Groups.|||
12546|Mount Bruce Supergroup|67721|6|Mentioned|p37, p38 Fig.9||||||Includes Hamersley Group and Fortescue Group.|||
12546|Mount Bruce Supergroup|67855|5|Briefly described|p210, 212 fig 3-10, p218, 231.|||Hamersley Basin.|||Includes Turee Creek Group, Hamersley Group, Fortescue Group|Unconformably overlain by Wyloo Group.||
12546|Mount Bruce Supergroup|68035|5|Briefly described|p284, Fig 1|Paleoproterozoic|Neoarchean|Apparently still a current name although the constituent Groups are now considered to be in separate basins.|2.78 - 2.21 Ga||Includes Fortescue, Hamersley and Turee Creek Groups.|||
12546|Mount Bruce Supergroup|68280|6|Mentioned|p1|||||||||
12546|Mount Bruce Supergroup|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|||Includes Fortescue Group.|||23-SEP-13
12546|Mount Bruce Supergroup|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2775-2715 Ma||Includes the Fortescue Group.|||
12546|Mount Bruce Supergroup|68283|5|Briefly described|Map Legend|Neoarchean|Archean|Marble Bar Sub-basin, Fortescue Basin.|||Includes Fortescue Group.|||
12546|Mount Bruce Supergroup|69012|5|Briefly described|Map Legend|Archean|Archean|Fortescue Basin.|||Includes the Fortescue Group.|||
12546|Mount Bruce Supergroup|69166|6|Mentioned|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Turee Creek Group|||
12546|Mount Bruce Supergroup|69167|6|Mentioned|geologyp_lut.csv|Neoarchean|Neoarchean||||Includes Hamersley Group, Fortescue Group|||
12546|Mount Bruce Supergroup|69185|5|Briefly described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.|||Includes Fortescue Group, Hamersley Group, Turee Group.|||
12546|Mount Bruce Supergroup|69299|5|Briefly described|p1, p7, p14, map||Archean|Only lower part preserved on COOYA POOYA 1:100 000 sheet|||Includes Fortescue Group, Hamersley Group.|||
12546|Mount Bruce Supergroup|69301|5|Briefly described|p21 Fig.8||||||Hamersley Group, Fortescue Group|Overlies De Grey Supergoup with regional unconformity.||
12546|Mount Bruce Supergroup|69411|6|Mentioned|p282|||Geological province: Pilbara Craton.|||Includes Fortescue Group.|||
12546|Mount Bruce Supergroup|69538|6|Mentioned|p516-517 Figs.2-3, p520, p559 Fig.34|Paleoproterozoic|Paleoproterozoic||||Includes Fortescue, Hamersley and Turee Creek Groups.|||
12546|Mount Bruce Supergroup|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.|||Fortescue, Hamersley, Turee Creek Groups.|Is overlain by Wyloo Group.||
12546|Mount Bruce Supergroup|69590|5|Briefly described|GEOL_LUT_CSV files|||Of Fortescue Basin. 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.|||Includes Fortescue Group, Hamersley Group.|||
12546|Mount Bruce Supergroup|69739|5|Briefly described|p69|||Myers (1993). Hamersley Basin.|2.8-2.4 Ga.||Fortescue, Hamersley, Turee Creek Groups.||Volcanic and sedimentary sequence.|
12546|Mount Bruce Supergroup|69745|6|Mentioned|p270-272|||Hamersley Province.|||Fortescue, Hamersley, Turee Creek Groups.|Is overlain unconformably by (Lower) Wyloo Group.||
12546|Mount Bruce Supergroup|70086|5|Briefly described|p195|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.|||Includes Turee Creek Group and Hamersley Group.|||
12546|Mount Bruce Supergroup|70775|6|Mentioned|p15||||||Includes the Fortescue Group.|||
12546|Mount Bruce Supergroup|70826|6|Mentioned|p6 tbl 2|||Turee Creek Basin, Hamersley Basin, Fortescue Basin.|||Turee Creek Group, Hamersley Group, upper and Hamersley Group, lower|||
12546|Mount Bruce Supergroup|70958|5|Briefly described|p2, 4|Paleoproterozoic|||||Includes Turee Creek Group.|||
12546|Mount Bruce Supergroup|71042|5|Briefly described|p65, p67|Paleoproterozoic|Neoarchean|||c. 2775-2450 Ma|Includes the Hamersley and Fortescue Groups.|||24-MAY-19
12546|Mount Bruce Supergroup|71112|5|Briefly described|p69-70,88|Archean|Archean|Geological province: Hamersley Province, Pilbara Craton. Records rifting of Archean Pilbara Craton.|~2.8 Ga||Includes Turee Creek, Hamersley and Fortescue groups.|||
12546|Mount Bruce Supergroup|71803|5|Briefly described|p366|||Pilbara Craton. Covers over 100,000km2 on the southern margin of the pilbara craton.|ca 2800-2400 Ma||Includes the Fortescue Group, Hamersley Group and the Turee Creek Group.|||
12546|Mount Bruce Supergroup|71808|4|Described|v, xiii, p5, p7, p10, p44, p99, p149|Palaeoproterozoic|Neoarchean|Hamersley Province. Overlies the Pilbara Craton.|||Includes the Fortescue Group, Hamersley Group and Turee Creek Group.||Weakly metamorphosed sedimentary and volcanic rocks.|
12546|Mount Bruce Supergroup|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Fortescue Group, Turee Creek Group.|||
12546|Mount Bruce Supergroup|72251|6|Mentioned|p53|Paleoproterozoic|Neoarchean|Geological province: Pilbara Craton.|2.77-2.43 Ga|||||
12546|Mount Bruce Supergroup|72254|6|Mentioned|App.A p10|Paleoproterozoic|Neoarchean|Basal unit is the Fortescue Group.|||Fortescue Group, Hamersley Group, Brockman Iron Formation, Joffre Member.|||
12546|Mount Bruce Supergroup|72447|6|Mentioned|p238|||[Written as Mt Bruce supergroup, p238 Fig.7].||||||
12546|Mount Bruce Supergroup|72493|5|Briefly described|p28|||Northern Hamersley Basin. Crops out mostly in the south of the Basin.|c.2.8 - 2.2 Ga.||Fortescue, Hamersley, Turee Creek Groups.||Granites and granitoids.|
12546|Mount Bruce Supergroup|72569|6|Mentioned|p2|||Unconformably overlies the Pilbara Craton. Of the Hamersley Basin.|ca. 2800-2400 Ma||Includes the Fortescue Group, Hamersley Group and the Turee Creek Group.|||
12546|Mount Bruce Supergroup|72570|6|Mentioned|p2-3||||||Includes the Turee Creek Group, Hamersley Group and the Fortescue Group.|||
12546|Mount Bruce Supergroup|72712|5|Briefly described|p1, 2, 3, 5, 6, p8-25, p31, 33, 35, 48.|Paleoproterozoic|Neoarchean|Shown on p63 (back cover summary).|||Fortescue Group, Hamersley Group and Turee Group|Underlies Wyloo, Capricorn, Shingle Creek, Mount Minnie and Bresnahan Groups. Intruded by dolerite sills and dykes.||
12546|Mount Bruce Supergroup|72758|5|Briefly described|p4 Fig.1, p6, p17-p28, p30-32, p38, p42|Archaean|Archaean|Established by Halligan and Daniels (1964), and revised by Trendall (1979) to incorporate the Fortescue Group, Hamersley Group, and Turee Creek Group.|2750 Ma to 2490 Ma depositional age||Fortescue Group, Hamersley Group, Turee Creek Group.|Intruded by dolerite sills.|Includes basalt, sandstone and other volcanics. Conglomerate, lithic ard quartzitic arenites, wacke, mudstone, pebble-cobble mudstone, dolomite, basalt intruded by dolerite sills. Includes BIF with chert, and podded chert.|
12546|Mount Bruce Supergroup|73022|6|Mentioned|p2|||Overlies the Pilbara Craton. Greenschist facies metamorphism along the southern margin of the supergroup with stronger folding and faulting.|||Hamersley Group, Fortescue Group, Turee Creek Group.||Volcano-sedimentary rocks with prehnite-pumpellyite grade metamorphism and minimal deformation.|
12546|Mount Bruce Supergroup|73160|6|Mentioned|p12|Neoarchean|Neoarchean|Overlies the southern Pilbara Craton. Contains bedding-parallel hydrothermal veins with monazite Pb/Pb  age of 2307 +/- 15 Ma and xenotime Pb/Pb age of 2097 +/- 5 Ma (Rasmussen et al., 2020).|2.63-2.5 Ga||||Includes shales.|
12546|Mount Bruce Supergroup|73538|6|Mentioned|p2 Fig. 1A, p3-4|||Uppermost unit is the Turee Creek Group.|||Hamersley Group, Turee Creek Group, Fortescue Group|||
12546|Mount Bruce Supergroup|75075|6|Mentioned|p420|Paleoproterozoic|Neoarchean|Pilbara Craton. Has undergone only low levels of metamorphism and alteration.|2.77-2.45 Ga.||Turee Creek, Hamersley, Fortescue Groups.|||
12573|Mount Cedric Lamproite|41158|6|Mentioned|Table 44|||||||||
12576|Mount Chandler Sandstone|22746|5|Briefly described|Fig.3 p515|Ordovician|Ordovician|Spelt Mt Chandler Sandstone||||||
12576|Mount Chandler Sandstone|22922|6|Mentioned|34|||||||||
12576|Mount Chandler Sandstone|23054|6|Mentioned|p36|||||||||25-MAR-21
12576|Mount Chandler Sandstone|23282|2|Defined|p80||Late Ordovician|Equiv to Pacoota Sandstone of Amadeus Basin. 'Mount Chandler Sandstone' introduced by Coats (1963), redefined by Benbow (1982). DO NOT CONFUSE WITH CHANDLER FORMATION OF AMADEUS BASIN. of Munda Group, Officer Basin. Age: Late Ordovician 457-450Ma.||||||06-SEP-06
12576|Mount Chandler Sandstone|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
12576|Mount Chandler Sandstone|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|Mount is Mt. in text.||||||
12576|Mount Chandler Sandstone|23818|5|Briefly described|p108|Ordovician|Ordovician|Presence of Scolithus and Cruziana fossils.||||||
12576|Mount Chandler Sandstone|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
12576|Mount Chandler Sandstone|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
12576|Mount Chandler Sandstone|24112|5|Briefly described|p254  Fig.2|Late Ordovician|Early Ordovician|Mount is spelt Mt. in text. Of the Munda Group. Geological Province: Officer Basin||||||
12576|Mount Chandler Sandstone|30075|6|Mentioned|p12|||||||||
12576|Mount Chandler Sandstone|30544|6|Mentioned|p49|||||||||
12576|Mount Chandler Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
12576|Mount Chandler Sandstone|30923|6|Mentioned|Map legend|Mesozoic|Paleozoic|Palaeozoic - Mesozoic||||||07-NOV-08
12576|Mount Chandler Sandstone|31457|6|Mentioned|p13|||||||||
12576|Mount Chandler Sandstone|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
12576|Mount Chandler Sandstone|31969|6|Mentioned|p9|||||||||
12576|Mount Chandler Sandstone|31972|6|Mentioned|p4|||Cambro-Ord. age relationships||||||
12576|Mount Chandler Sandstone|32431|5|Briefly described|p99|||||||||
12576|Mount Chandler Sandstone|33491|6|Mentioned|p55|||||||||
12576|Mount Chandler Sandstone|33523|6|Mentioned|p20|||||||||
12576|Mount Chandler Sandstone|33578|6|Mentioned|p77|||Ordovician||||||
12576|Mount Chandler Sandstone|33738|6|Mentioned|p58|||||||||
12576|Mount Chandler Sandstone|34280|6|Mentioned|p10|||L.Ord.||||||
12576|Mount Chandler Sandstone|34610|6|Mentioned|p178|||Ordovician||||||
12576|Mount Chandler Sandstone|34612|3|Fully described|p111|||Ordovician. P108. Fossils P111.||||||
12576|Mount Chandler Sandstone|35149|6|Mentioned|Table 4|||||||||
12576|Mount Chandler Sandstone|35628|4|Described|Table 3|||||||||
12576|Mount Chandler Sandstone|36096|6|Mentioned|Fig.3|||||||||
12576|Mount Chandler Sandstone|36128|6|Mentioned|p13|||||||||
12576|Mount Chandler Sandstone|36491|6|Mentioned|Fig.2|||||||||
12576|Mount Chandler Sandstone|36920|6|Mentioned|Table 1|||||||||
12576|Mount Chandler Sandstone|38022|6|Mentioned|Fig.4|||||||||
12576|Mount Chandler Sandstone|38329|1|Redefined|p208|Ordovician|Ordovician|See also P194.||||||
12576|Mount Chandler Sandstone|39352|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
12576|Mount Chandler Sandstone|40003|5|Briefly described|Table 15|||||||||
12576|Mount Chandler Sandstone|40136|5|Briefly described|p32|||||||||
12576|Mount Chandler Sandstone|40926|6|Mentioned|p11|||||||||
12576|Mount Chandler Sandstone|40945|6|Mentioned|Fig.3|||||||||
12576|Mount Chandler Sandstone|43052|5|Briefly described|p198|||||||||
12576|Mount Chandler Sandstone|43053|5|Briefly described|Map Legend|Devonian|Ordovician|Spelt Mt Chandler Sandstone. Of the "Munda Sequence". Shallow marine to deltaic sandstone, siltstone and shale.||||||25-MAY-05
12576|Mount Chandler Sandstone|43258|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
12576|Mount Chandler Sandstone|43298|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
12576|Mount Chandler Sandstone|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
12576|Mount Chandler Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
12576|Mount Chandler Sandstone|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
12576|Mount Chandler Sandstone|43743|6|Mentioned|Fig.2,p33||Ordovician|||||||
12576|Mount Chandler Sandstone|44109|5|Briefly described|p22 Fig. 22|Ordovician|Ordovician|Geological Province: central Officer Basin. Mount is Mt in text of figure.||||||
12576|Mount Chandler Sandstone|44133|4|Described|p40, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Gradationally overlies Byilkaoora Formation. Disconformably overlies: Trainor Hill Sandstone, Marla Group. Correlated with Boongar beds.||||||07-NOV-08
12576|Mount Chandler Sandstone|44535|4|Described|map legend||Ordovician|(G/53-9).||||||
12576|Mount Chandler Sandstone|45149|6|Mentioned|p43|||See also Table 1.||||||
12576|Mount Chandler Sandstone|49792|5|Briefly described|Fig.5|||||||||
12576|Mount Chandler Sandstone|60953|5|Briefly described|Map Legend|Silurian|Silurian|Of the Munda Group. Mount is Mt in text.||||||27-APR-05
12576|Mount Chandler Sandstone|61108|5|Briefly described|map legend|Silurian|Silurian|Spelt Mt on map legend. Of Munda Group. Shallow marine to fluviodeltaic sandstone, siltstone and shale. Age: ?Silurian.||||||02-JUN-05
12576|Mount Chandler Sandstone|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Geological Province: Officer Basin. Mount is Mt in text.||||||10-AUG-07
12576|Mount Chandler Sandstone|65313|5|Briefly described|p578, p580 Fig. 8|Early Ordovician|Late Cambrian|Officer Basin. Ungoolya 1 well.||Of Munda Group.||Overlies Table Hill and Kulyong Volcanics (484 +/- 4 Ma and 483.6 +/- 20 Ma K-Ar dates); underlies Indulkana Shale.||26-MAR-12
12576|Mount Chandler Sandstone|69445|5|Briefly described|p30:5-6, 17|||Officer Basin.||||Overlies Kulyong Formation (now Table Hill Volcanics).||12-JUL-16
12576|Mount Chandler Sandstone|71146|5|Briefly described|p6|Late Ordovician|Middle Ordovician|Officer Basin.||Munda Group||Unconformably overlies the Table Hill Volcanics. Overlain by the Indulkana Shale and Blue Hills Sandstone.|Sandstone.|
12576|Mount Chandler Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
12576|Mount Chandler Sandstone|72478|5|Briefly described|p8|Late Ordovician|Early Ordovician|Officer Basin.|c. 495 Ma-450 Ma|Munda Group|Includes the Byilkaoora Member.|Overlies the Kulyong Formation. Underlies the Indulkana Shale.||25-MAR-21
12576|Mount Chandler Sandstone|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Sandstone, well-rounded, fine- to medium-grained quartz; sandstone, feldspathic, burrowed.|
12576|Mount Chandler Sandstone|73099|5|Briefly described|Map legend.|Ordovician|Ordovician|Officer Basin.||Munda Group.|||Pale grey and white to orange-brown (weathered), kaolinitic, very fine to coarse quartz sandstone with thin interbeds of white to dark red-brown claystone and siltstone.|
12576|Mount Chandler Sandstone|73109|5|Briefly described|Map legend.|Devonian|Ordovician|Subcrop and minor outcrop.|||||Orange-brown, very fine- to fine-grained quartz sandstone, bioturbated in part.|
12593|Mount Corlac Ultramafics|41066|5|Briefly described|p34|||Mention 1 of 2 E15||||||
12593|Mount Corlac Ultramafics|42289|5|Briefly described|p30|||Also Fig.1 P29||||||
12602|Mount Crofton Granite|23414|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|||||||
12602|Mount Crofton Granite|23758|4|Described|p11|Neoproterozoic|Neoproterozoic|Age: 639+/-9 Ma and 678+/-12 Ma (SHRIMP U-Pb).||||||09-DEC-08
12602|Mount Crofton Granite|24197|5|Briefly described|p26, p102 Tb. 14.1|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
12602|Mount Crofton Granite|24594|5|Briefly described|p608 Fig. 4|Neoproterozoic|Mesoproterozoic|Age: ~850-650Ma (Pb-Pb isochron, McNaughton and Goellnicht 1990).  Geological Province: Paterson Orogen.||||||27-SEP-12
12602|Mount Crofton Granite|30484|6|Mentioned|p56|||Re age dates||||||
12602|Mount Crofton Granite|35902|6|Mentioned|p7|||||||||
12602|Mount Crofton Granite|39697|6|Mentioned|p210|||||||||
12602|Mount Crofton Granite|41158|6|Mentioned|p19|||||||||
12602|Mount Crofton Granite|41892|6|Mentioned|p313|||||||||
12602|Mount Crofton Granite|41946|5|Briefly described|p103|||||||||
12602|Mount Crofton Granite|42754|6|Mentioned|p3|||||||||
12602|Mount Crofton Granite|43348|6|Mentioned|P15|||Age is 620Ma||||||
12602|Mount Crofton Granite|43832|6|Mentioned|88-89||Neoproterozoic|Neoproterozoic age of 700 Ma||||||
12602|Mount Crofton Granite|43862|5|Briefly described|p383|||?Same as Mount Crofton Granite Complex.||||||09-DEC-08
12602|Mount Crofton Granite|43868|5|Briefly described|p153,p161|||Actually spelt Mt Crofton Granite on Figure . Age 690+/-48 Ma Pb-Pb, 614+/-42 Ma Rb-Sr.||||||
12602|Mount Crofton Granite|44139|6|Mentioned|p280, 282|Cryogenian|Cryogenian|Trendall (1974). 688+/-32 Ma (Pb-Pb isochron age: Goellnicht et al. 1988). Similar monzogranite intrudes Broadhurst Formation. Final tectonic event in the Paterson Orogen.|| ||||05-MAR-18
12602|Mount Crofton Granite|50436|5|Briefly described|p1.3, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the Mount Crofton Group (O'Callaghans Supersuite). Age: 614 +/- 8Ma (U-Pb).||||||
12602|Mount Crofton Granite|50621|5|Briefly described|p167|||Mount is Mt in text. Geological Province: Yeneena Basin (Paterson Orogen).||||||
12602|Mount Crofton Granite|60470|6|Mentioned|p9|Cryogenian|Cryogenian|Intrudes Wilki Formation. Age ~654 Ma. Post-dates Miles Orogeny structures.||||||
12602|Mount Crofton Granite|64580|4|Described|map legend||Neoproterozoic|Syenogranite and monzogranite.||||||09-DEC-08
12602|Mount Crofton Granite|64725|6|Mentioned|p57.|||Paterson Orogen.|c.650 Ma.|||||
12602|Mount Crofton Granite|64943|5|Briefly described|p25 Table 4, p26, 30|Neoproterozoic|Neoproterozoic|c. 620 Ma by SHRIMP U-Pb (Nelson 1995); 690+/-48 Ma by Pb/Pb (Goellnicht et al. 1991); 601+/-42 Ma by Rb-Sr (Williams 1992). Intrudes Lamil Group.||||||
12602|Mount Crofton Granite|65403|5|Briefly described|p29.|||Discrete circular to ovoid plutons. Intrusion post-dates Miles Orogeny D4 event.  Previous dates are Rb-Sr age of 598 +/- 24 Ma (Trendall 1974) and Pb-Pb age of 690 +/- 48 Ma (McNaughton and Goellnicht 1990). Referred to as Mount Crofton Granite 'Complex' p18.|621 +/- 13 Ma (SHRIMP U-Pb zircon; Nelson 1995).|||Intrudes Lamil Group.|Weakly-foliated granitoid.|
12602|Mount Crofton Granite|65455|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Within the Proterozoic Paterson Province. Contains clusterings of geochemical analyses with high U.||||||09-MAY-12
12602|Mount Crofton Granite|65725|5|Briefly described|Map legend|Cryogenian|Cryogenian|Medium grained, equigranular leucocratic syenogranite, and medium to coarse grained, equigranular to porphyritic biotite monzogranite. Age: ~654 Ma||||||30-NOV-11
12602|Mount Crofton Granite|65826|4|Described|p8 Fig.5, pp14-15. |Proterozoic|Proterozoic|Well exposed in several prominent hills in the northeastern map area. Forms thin laccolithic sheets, with the intruded Wilki Formation forming domes above and synforms around the margins. SHRIMP U-Pb ages of 640 +/- 8 Ma and 654 +/- 8 Ma are regarded as more reliable, given the extremely high concentration of uranium in the zircon crystals which gave ages (of the same samples) from 630 to 600 Ma due to lead loss from the damaged crystal structure.|c.654 Ma (Dunphy and McNaughton 1998).||||Predominantly medium- to coarse-grained biotite monzogranite, with local porphyritic phases; and medium-grained, equigranular leucocratic syenogranite; minor aplite and pegmatite dykes.|
12602|Mount Crofton Granite|67202|4|Described|p6, p57, p60-61, p63, p118, p189, p191|||See also p221, p224, p254, p256, p258-259, p261. Extends northwards into the Anketell Shelf region. Uranium-bearing rocks have potential as source for sandstone U deposits. Also appears as Mount Crofton Granite Suite on p57, p63, p221, p224, p254, p256, p259, p261. Gravity and aeromagmetic interpretation. Geochronology by Dunphy and McNaughton (1998). A unit in the Mount Crofton group of granites (a subdivision of the O'Callaghans Supersuite by Goellnicht et al., 1991). Shortened to Crofton Granite on p191 and Crofton Granites on p202. SHRIMP titanite age; other ages given.|654 +/- 8 Ma (Dunphy and McNaughton, 1998).|||Intrudes Lamil Group.||
12602|Mount Crofton Granite|68902|6|Mentioned|p8, p14-17, p23|Neoproterozoic|Neoproterozoic|Mount Crofton Suite?||||||
12602|Mount Crofton Granite|69590|4|Described|500k_geologyp08_lut.csv||Neoproterozoic||||||Undivided; syenogranite and monzogranite|
12602|Mount Crofton Granite|70826|6|Mentioned|p11|Neoproterozoic|Neoproterozoic|Rudall Province.||||||
12602|Mount Crofton Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, granophyre, monzogranite|
12602|Mount Crofton Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Paterson Orogen.|Max age 633+/-13 Ma, min 621+/-13 Ma.||||Syenogranite and monzogranite.|
12618|Mount Danvers Granodiorite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Boolaloo Supersuite.||||||07-FEB-11
12618|Mount Danvers Granodiorite|42260|6|Mentioned|p114|||||||||
12618|Mount Danvers Granodiorite|42435|6|Mentioned|Fig.1 P43|||||||||
12618|Mount Danvers Granodiorite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Boolaloo Supersuite. Underlies: Bangemall Group (unconformably).||||||07-NOV-08
12618|Mount Danvers Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
12618|Mount Danvers Granodiorite|72758|6|Mentioned|p4 Fig.1, p10 Tb.1, p43, p46.|||Named by Daniels (1965). Appears to be a sheet-like body, whose margins are parallel to the schistosity in the country rocks. It was probably emplaced by progressively wedging aside the pre-existing foliation of the host rocks.||||Intrudes Ashburton Formation, Morrisey Metamorphic Suite.|Mainly medium- to coarse-grained biotite granodiorite. Biotite granodiorite, mainly coarse-grained, contains mafic xenoliths.|
12642|Mount Dove Complex|41594|6|Mentioned|p70|||||||||
12660|Mount Dugel paragneiss|41942|5|Briefly described|p55|||||||||
12706|Mount Falconer Adamellite|32010|6|Mentioned|p168|||||||||
12710|Mount Fingall Dolerite|40005|6|Mentioned|p21|||Used in unpublished reports||||||
12730|Mount Gardner Adamellite|33272|6|Mentioned|Fig.2|||||||||
12730|Mount Gardner Adamellite|33274|6|Mentioned|p219|||||||||
12730|Mount Gardner Adamellite|33275|4|Described|p103|||See also PP104 - 108. Pet. min. & petrogenesis||||||
12767|Mount Gratwick Granodiorite|35641|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
12767|Mount Gratwick Granodiorite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
12767|Mount Gratwick Granodiorite|39697|3|Fully described|p40|||||||||
12767|Mount Gratwick Granodiorite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||100 sq. km. Mis-spelt as Mount Gatwick Granodiorite on p149.||Yule Granitoid Complex|||Leucogranodiorite, leucodiorite with amphibolite xenoliths.|
12779|Mount Hall-Carlow Castle Complex|39697|4|Described|p76|||||||||
12779|Mount Hall-Carlow Castle Complex|41594|6|Mentioned|p42|||||||||
12779|Mount Hall-Carlow Castle Complex|70312|6|Mentioned|p2|||West Pilbara Block. Occurs SE and SW of Roebourne. Approx. 2km thick, with an area of 150 km2.|||||Sheets of dunite, peridotite, pyroxenite, gabbro and minor anorthosite.|
12780|Mount Harris Basalt|22561|4|Described|p15|Neoproterozoic|Neoproterozoic|||||||
12780|Mount Harris Basalt|22567|6|Mentioned|p91|||||||||
12780|Mount Harris Basalt|22804|6|Mentioned|Fig 2 on p432|||Mount spelt Mt in text.||||||
12780|Mount Harris Basalt|23361|5|Briefly described|16 Fig.4|Neoproterozoic|Neoproterozoic|||||||
12780|Mount Harris Basalt|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Mount written Mt in text. Geological Province: Musgrave Block.||||||
12780|Mount Harris Basalt|30389|6|Mentioned|p9|||Refers Forman(1966)||||||
12780|Mount Harris Basalt|30390|6|Mentioned|p195|||||||||
12780|Mount Harris Basalt|30817|6|Mentioned|p11|||||||||
12780|Mount Harris Basalt|31393|6|Mentioned|Pl.25|||||||||
12780|Mount Harris Basalt|31970|6|Mentioned|p15|||||||||
12780|Mount Harris Basalt|33307|6|Mentioned|Fig.6|||||||||
12780|Mount Harris Basalt|33478|6|Mentioned|Table 1|||||||||
12780|Mount Harris Basalt|35102|6|Mentioned|Fig.2|||||||||
12780|Mount Harris Basalt|35308|6|Mentioned|Table 1|||||||||
12780|Mount Harris Basalt|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12780|Mount Harris Basalt|36887|6|Mentioned|p208|||||||||
12780|Mount Harris Basalt|39210|6|Mentioned|p40|||See also Fig.10.||||||09-NOV-06
12780|Mount Harris Basalt|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession.||||||09-NOV-06
12780|Mount Harris Basalt|42504|5|Briefly described|p67|||||||||
12780|Mount Harris Basalt|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|In the south-west.  Greenschist, basalt, tuff, conglomerate, quartzite.  Geological province: Amadeus Basin.||||||07-NOV-08
12780|Mount Harris Basalt|43503|6|Mentioned|12-50||Proterozoic|||||||
12780|Mount Harris Basalt|44139|6|Mentioned|p284|||Of Forman, 1966. Later Mount Harris Volcanics (Daniels, 1974); see references p284-286.|| ||||05-MAR-18
12780|Mount Harris Basalt|44493|4|Described|p.7, map||Precambrian|BLOOD RANGE sheet (G53-3). See p.9-12,14, for details. PreC.||||||09-NOV-06
12780|Mount Harris Basalt|44494|14|Not recorded|map legend|||||||||
12780|Mount Harris Basalt|45041|5|Briefly described|p15|||Precambrian||||||
12780|Mount Harris Basalt|48863|14|Not recorded|p.13|||||||||
12780|Mount Harris Basalt|48864|2|Defined|p.9,11-12||Proterozoic|Tb.1. On many pages. p.1,14,18,20-23,37,41,42,47,50,Pl.2,11,12. Middle or Upper Proterozoic. (G52-3,7).||||||
12780|Mount Harris Basalt|48963|6|Mentioned|Fig.3|||||||||
12780|Mount Harris Basalt|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Underlies Dean Quartzite.  Of the Tjauwata Group.||||||22-DEC-09
12780|Mount Harris Basalt|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Intruded by Walu Granite.||||||09-JUN-04
12780|Mount Harris Basalt|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Variably silicified and epidotised, amygdaloidal basalt.  Geological Province: Musgrave Block.||||||
12780|Mount Harris Basalt|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Basalt. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
12780|Mount Harris Basalt|60683|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|Age: 1070-1040Ma.  Geological Province: Musgrave Block. Mount may be Mt in text.||||||20-APR-05
12780|Mount Harris Basalt|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Gp. Distinctively banded rock due to alternating layers silicified and epidotised amygdaloidal basalt with less altered basalt. Over Tjuninanta Fn; under Puntitjata Rhyolite. Intruded by veins of Walu Granite. Thick: 1-2km (est.). Mount is Mt||||||19-JUL-05
12780|Mount Harris Basalt|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin. Mount is Mt in text.||||||06-FEB-08
12780|Mount Harris Basalt|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Variably silicified and epidotised amygdaloidal basalt with rare lenses of crystalline quartz sandstone.||||||23-DEC-09
12780|Mount Harris Basalt|62359|5|Briefly described|p547, p549|||Underlies Dean Quartzite. Geological Province: Amadeus Basin. Basaltic bimodal volcanics. Mount may be Mt in text.||||||
12780|Mount Harris Basalt|62609|5|Briefly described|Map Legend|Precambrian|Precambrian|Green Schist, basalt, tuff, conglomerate, quartzite.||||||
12780|Mount Harris Basalt|62620|5|Briefly described|Map Legend|Precambrian|Precambrian|Green schist, basalt, tuff, conglomerate, quartzite.||||||
12780|Mount Harris Basalt|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Gp. Overlies Tjuninanta Fm. Max. thick:2km. Accumulated basalt flows. Geochemically similar to Mummawarrawarra Basalt (Tollu Group), Alcurra dolerite and Giles Complex rocks; interpreted as extrusive phase of the Giles Complex. Age: 1080Ma.||||||07-FEB-08
12780|Mount Harris Basalt|63562|6|Mentioned|p341|||Of Amadeus Basin. Part of the initial Basin fill.||Tjauwata Group||Correlated with Stuart Dyke Swarm.||
12780|Mount Harris Basalt|63866|5|Briefly described|p203, p208|||Mulga Park Domain, Musgrave Province.||Tjauwata Group||Overlain by the Puntitjata Rhyolite. Intruded by the Walu Granite.||
12780|Mount Harris Basalt|64580|4|Described|map legend||Mesoproterozoic|Of Tjauwata Group. Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.||||||09-DEC-08
12780|Mount Harris Basalt|65233|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Overlies Tjuninanta Formation; overlain by Bloods Range Formation. Age: 1080Ma. Max. thickness: 2km. Geological province: Amadeus Basin. Basaltic flows.||||||07-FEB-11
12780|Mount Harris Basalt|65256|1|Redefined|p3, p6 Tb.1, p9-11, p20, p27, p37-39|Stenian|Stenian|Redefined. Estimated to be 1-2 km thick minimum. Correlative of Mummawarrawarra Basalt; intruded by Walu Granite and Alcurra dolerite. Largely non-magnetic; associated with shallow Cenozoic and Quaternary soils; interpreted magmatic age of 1080 Ma. Similar in composition to Alcurra dolerite. Forms rounded low hills and peneplains.||Of the Tjauwata Group.||Overlies Tjuninanta Formation (gradational contact), and Karukali Quartzite. Overlain by Puntitjata Rhyolite or Bloods Range Formation.|Amygdaloidal basalt with layered altered (epidotised and silicified) and unaltered zones and with rare crystalline quartz sandstone interbeds; no quartz-feldspar porphyry subunit.|19-MAY-14
12780|Mount Harris Basalt|65906|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|Unit in Tjauwata Group. A correlative of Mummawarrawarra Basalt.  Is intruded by  Walu Granite aged 1084 +/- 9 Ma (SHRIMP U-Pb zircon).||||||
12780|Mount Harris Basalt|67128|5|Briefly described|p12, p18|||||Tjauwata Group.||Is intruded by Walu Granite. Correlated (tentatively) with Mummawarrawarra Basalt.||
12780|Mount Harris Basalt|68995|6|Mentioned|p6|||||Tjauwata Group||||
12780|Mount Harris Basalt|69091|5|Briefly described|p70, p103 Fig.5.6|||These are basal units of Bentley Supergroup (Howard et al., 2011a; Evins et al., 2010).||Tjauwata Group||Equivalent to Mummawarrawarra Basalt (of Kunmarnara Group).||07-OCT-14
12780|Mount Harris Basalt|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite|
12780|Mount Harris Basalt|69436|4|Described|p21:4, 11, 13-14, 19, 21|Mesoproterozoic|Mesoproterozoic|Forman (1966). Musgrave Province. Origin of magma discussed; similar geochemistry as Alcurra Dolerite suggests a common source. Very thick: estimated at 1-2 km. Is locally thrust over Dean Quartzite. Contains a quartz vein with Au, Ag and secondary lead and copper minerals.||Tjauwata Group.||Overlies Tjuninanta Formation. Is overlain by, or laterally equivalent to, Puntitjata Rhyolite. Is intruded by Walu Granite. Correlated with Mummawarrawarra Basalt.|Distinctively banded basalts, due to alternating layers of silicified and epidotised amygdaloidal basalt with less altered basalt. Fe-tholeiites.|12-JUL-16
12780|Mount Harris Basalt|69729|5|Briefly described|p79|||||Tjauwata Group.||Equivalent to the Mummawarrawarra Basalt.||
12780|Mount Harris Basalt|70018|4|Described|p233,235-237|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Minimum age provided by the 1084+\-9 Ma age of high level granites that intrude it (U-Pb on zircon; Close et al., 2003).||Unit of Tjauwata Group.||Overlain by, or laterally equivalent to Puntitjata Rhyolite. Underlain by Tjuninanta Formation.|Epidotised, silicified amygloidal basalt flows, rare quartz sandstone beds.|
12780|Mount Harris Basalt|70634|4|Described|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic|||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.|
12780|Mount Harris Basalt|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 siliciclastic sedimentary and volcanic rocks|
12780|Mount Harris Basalt|71210|6|Mentioned|p8|||||Tjauwata Group||||
12780|Mount Harris Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greenschist facies rock, basalt|
12780|Mount Harris 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). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1084-1075 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite|
12780|Mount Harris Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Tjauwata Group|||Metamorphosed basalt, basaltic tuff, conglomerate, and quartzite.|
12780|Mount Harris Basalt|72094|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Bentley Basin.||Unit of Tjauwata Group.||Conformably underlain by Karukali Quartzite. Likely time and lateral equivalent to Mummawarrawarra Basalt.||
12803|Mount House Group|22547|6|Mentioned|p26||Neoproterozoic|||||||
12803|Mount House Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
12803|Mount House Group|22754|5|Briefly described|p12|Neoproterozoic|Neoproterozoic|Age: 670 Ma||||||
12803|Mount House Group|23383|6|Mentioned|p20|||Correlated with Louisa Downs Group (Coates & Preiss 1980). Plumb (1996) prefers correlation with Kuniandi Group.||||||25-JAN-05
12803|Mount House Group|23599|6|Mentioned|p16|Neoproterozoic|Neoproterozoic|||||||
12803|Mount House Group|23722|5|Briefly described|p23|Neoproterozoic|Neoproterozoic|Age: c.670Ma||||||
12803|Mount House Group|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Mount is Mt in text.||||||
12803|Mount House Group|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: c. 610 Ma. Glacigene rocks; tillite, sandstone, siltstone and minor stromatolitic dolomite.||||||
12803|Mount House Group|29591|6|Mentioned|p121|||||||||
12803|Mount House Group|30525|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12803|Mount House Group|30533|4|Described|p21|||On Table 5||||||
12803|Mount House Group|30894|5|Briefly described|p250|||Adelaidean||||||
12803|Mount House Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12803|Mount House Group|30896|4|Described|p18|||||||||
12803|Mount House Group|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
12803|Mount House Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12803|Mount House Group|32660|4|Described|Table 6|||||||||
12803|Mount House Group|32664|6|Mentioned|Map legend|Proterozoic|Proterozoic|Mention in notes||||||
12803|Mount House Group|32728|6|Mentioned|Fig.3|||||||||
12803|Mount House Group|34462|4|Described|p10|||See Table 1. Adelaidean||||||
12803|Mount House Group|34463|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12803|Mount House Group|36551|6|Mentioned|Table 10|||||||||
12803|Mount House Group|36888|4|Described|p213|||||||||
12803|Mount House Group|36898|6|Mentioned|p192|||||||||
12803|Mount House Group|37462|4|Described|Table 4.X|||||||||
12803|Mount House Group|37927|6|Mentioned|p504|||||||||
12803|Mount House Group|38157|6|Mentioned|Table X|||||||||
12803|Mount House Group|38243|6|Mentioned|p357|||||||||
12803|Mount House Group|38988|6|Mentioned|Fig.4|||||||||
12803|Mount House Group|39210|5|Briefly described|p49|||||||||
12803|Mount House Group|40105|6|Mentioned|p313|||||||||
12803|Mount House Group|41453|6|Mentioned|p244|||||||||
12803|Mount House Group|42149|5|Briefly described|Table 1 P709|||||||||
12803|Mount House Group|42710|5|Briefly described|map legend|Proterozoic||||||||
12803|Mount House Group|42811|3|Fully described|p30|||||||||
12803|Mount House Group|42814|6|Mentioned|p16|||||||||
12803|Mount House Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
12803|Mount House Group|43595|6|Mentioned|p550|||||||||
12803|Mount House Group|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
12803|Mount House Group|44140|5|Briefly described|p300, p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount House area. Associated with the 670 Ma Marinoan glaciation.|||Includes Walsh Tillite, Traine Formation, Throssell Shale and Estaughs Formation.||Tillite, siltstone, sandstone, shale, dolomite.|07-MAR-18
12803|Mount House Group|44155|6|Mentioned|p254 Fig.3-40|Neoproterozoic|Neoproterozoic|Kimberley region.||||||
12803|Mount House Group|44363|14|Not recorded|p.13||Proterozoic|Unconformably overlies Bastion Group.||||||15-AUG-05
12803|Mount House Group|44367|14|Not recorded|map legend||Adelaidean|(Reprinted 1971).||||||
12803|Mount House Group|48927|6|Mentioned|Table 1|||Equiv. Kuniandi Gp. unconformably on Carpentarian||||||
12803|Mount House Group|48931|3|Fully described|p59|||||||||
12803|Mount House Group|60724|5|Briefly described|p5 Fig. 2|Neoproterozoic|Neoproterozoic|Age: ~670Ma.||||||
12803|Mount House Group|61571|5|Briefly described|p654 Fig. 1|Neoproterozoic|Neoproterozoic|Includes the Walsh Tillite. Glacigene deposits. Overlies the Kimberley Group. Geological Province: Kimberley Basin.||||||04-MAY-06
12803|Mount House Group|62453|6|Mentioned|p67|||||||||
12803|Mount House Group|63458|6|Mentioned|p872-873 Figs.1,2, p874, p897 Fig.19|Ediacaran|Cryogenian|Mount House area, west Kimberley region.|||Includes Walsh Tillite, Traine and Estaughs Formations, and Throssell Shale.|||
12803|Mount House Group|63762|5|Briefly described|p19|||||||||07-FEB-11
12803|Mount House Group|64104|6|Mentioned|p70 fig 7|Neoproterozoic|Neoproterozoic|||||||
12803|Mount House Group|64580|4|Described|map legend|Ediacaran|Ediacaran|Tillite, sandstone, siltstone, and minor stromatolitic dolomite.||||||09-DEC-08
12803|Mount House Group|64635|6|Mentioned|p2 Fig.1|||||||||
12803|Mount House Group|64733|6|Mentioned|p169 Fig.1|Neoproterozoic|Neoproterozoic|?Kimberley Basin.||||||20-APR-12
12803|Mount House Group|67620|6|Mentioned|p2-3|Neoproterozoic|Neoproterozoic|||||||
12803|Mount House Group|68138|6|Mentioned|p154|Neoproterozoic|Neoproterozoic|||||||
12803|Mount House Group|68244|4|Described|p659-662|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. Up to c. 540m thick (Derrick and Playford 1973).||Unit of Mount House Group.|Includes Estaughs Formation, Throssell Shale, Traine Formation and Walsh Formation.|Underlain unconformably by Kimberley Group.||
12803|Mount House Group|68473|6|Mentioned|p530|Neoproterozoic|Neoproterozoic|Kimberley region.||||||
12803|Mount House Group|68733|6|Mentioned|p176 Fig.1|||||||||
12803|Mount House Group|69003|6|Mentioned|vi, p5, p65, p72|||Halls Creek Orogen. Overlies the Kimberley Basin succession.||||||
12803|Mount House Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Mount House Sub-basin, Louisa Basin. See info in 500k_geologyp08_lut.csv|||Includes Throssell Shale, Traine Formation, Walsh Tillite.||Tillite, sandstone, siltstone, and minor stromatolitic dolomite.|03-AUG-15
12803|Mount House Group|69165|4|Described|500k_geologyp08_lut.csv|Ediacaran|Ediacaran||||||Undivided; tillite, sandstone, siltstone and minor stromatolitic dolomite.|
12803|Mount House Group|69437|6|Mentioned|p22:1|||Centralian A Superbasin (Centralian Superbasin of Walter et al., 1995).||||||12-JUL-16
12803|Mount House Group|69585|6|Mentioned|p17|Neoproterozoic|Neoproterozoic|||||Unconformably overlies Pentecost Sandstone.||
12803|Mount House Group|69597|6|Mentioned|p2, p5 fig 2b|Ediacaran|Cryogenian||635-560 Ma|||||
12803|Mount House Group|69634|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Mount House Sub-basin, Louisa Basin, Centralian Superbasin. See 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|||Includes Walsh Tillite, Throssell Shale, Traine Formation.||Undivided; tillite, sandstone, siltstone, and minor stromatolitic dolomite|
12803|Mount House Group|69660|5|Briefly described|Map legend|Ediacaran|Cryogenian|Louisa Basin, North Australian Craton.|||Includes Walsh Tillite, Traine Formation, Throssell Shale.||Tillite, sandstone, siltstone, shale, dolostone.|
12803|Mount House Group|70154|6|Mentioned|250k_geologyp_lut.csv|Ediacaran|Cryogenian|See also 250k_interpgeop_lut.csv.|||Includes Traine Formation, Throssell Shale, Walsh Tillite|||
12803|Mount House Group|70731|5|Briefly described|p268,278|Neoproterozoic|Neoproterozoic|Geological province: King Leopold Orogen and Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||Equivalent to Louisa Downs and Albert Edward groups.||
12803|Mount House Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
12803|Mount House Group|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|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 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 1m_interpgeop_lut.csv.|720-541 Ma (inferred)||Includes Estaughs Formation, Throssell Shale, Traine Formation, Virgin Hills Formation, Walsh Tillite.||Tillite, sandstone, siltstone, and minor stromatolitic dolomite|
12803|Mount House Group|71302|6|Mentioned|p4|||Of Kimberley and Speewah basins.||||||
12803|Mount House Group|71811|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Louisa Basin.|||Walsh Tillite; Traine, Estaughs Formations; Throssell Shale.|||
12803|Mount House Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Cryogenian|Louisa Basin.|||||Tillite, sandstone, siltstone, and minor stromatolitic dolomite.|
12803|Mount House Group|73086|6|Mentioned|p4 Fig.4|||||||||
12813|Mount Ibis Lamproite|41158|6|Mentioned|Table 45|||||||||
12840|Mount John Shale Member|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
12840|Mount John Shale Member|32660|6|Mentioned|p223|||||||||
12840|Mount John Shale Member|32728|6|Mentioned|Fig.3|||||||||
12840|Mount John Shale Member|36885|4|Described|p177|||||||||
12840|Mount John Shale Member|37371|6|Mentioned|p388|||||||||
12840|Mount John Shale Member|37462|4|Described|Table 4.VI|||||||||
12840|Mount John Shale Member|38157|6|Mentioned|Table X|||||||||
12840|Mount John Shale Member|44155|4|Described|p251-252|||200m thick.|1128 +/- 110 Ma (Dow and Gemuts, 1969).|Wade Creek Sandstone|||Khaki and some black shale and siltstone, minor quartz sandstone; some beds highly ferruginous.|
12840|Mount John Shale Member|44317|4|Described|Table 3||Adelaidean|||||||
12840|Mount John Shale Member|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
12840|Mount John Shale Member|45047|2|Defined|p80|Adelaidean|Adelaidean|See also pp32,35.||||||28-MAY-15
12840|Mount John Shale Member|45112|6|Mentioned|p30|||||||||
12840|Mount John Shale Member|45140|5|Briefly described|p59||||1128 +/- 110 Ma (Dow and Gemuts, 1969).|Wade Creek Sandstone.|||A thick shale lens.|
12840|Mount John Shale Member|48938|5|Briefly described|p76|||Age. Refers Dow & Gemuts (1969).||||||
12840|Mount John Shale Member|67484|5|Briefly described|p294|Neoproterozoic||Kimberley Region. Previously, Sprigg (1949) named the possible fossil Protoniobia wadea from this unit and considered it to be related to the Ediacaran fauna from South Australia. The age and organic nature are questionable.||||Is overlain by Eliot Range Dolomite.||28-MAY-15
12840|Mount John Shale Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Victoria River Basin||Wade Creek Formation|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone.|03-AUG-15
12840|Mount John Shale Member|69165|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|||Wade Creek Formation|||Grey-green siltstone, mudstone and fine to coarse grained sandstone.|
12840|Mount John Shale Member|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Victoria River Basin. Events:Alice Springs Orogeny; Yampi Orogeny D1/M1.|1600-1000 Ma (Inferred)|Unit of Wade Creek Formation.|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone|
12840|Mount John Shale Member|70154|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1000-1600 Ma||||Siltstone, mudstone and fine to coarse grained sandstone.|
12840|Mount John Shale Member|71267|5|Briefly described|100k_interpgeop_lut.csv|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).|1600-1000 Ma (inferred)|Unit of Wade Creek Formation.|||Grey-green siltstone, mudstone, and fine- to coarse-grained sandstone|
12840|Mount John Shale Member|73255|6|Mentioned|p534 Fig.2|Tonian|Tonian|Written as Mt John Shale Member in text.||Wade Sandstone||Interbedded in the Wade Sandstone.||
12864|Mount Keith Granodiorite|23281|6|Mentioned|p6|||||||||
12864|Mount Keith Granodiorite|29784|6|Mentioned|p27|||||||||
12864|Mount Keith Granodiorite|32011|6|Mentioned|p151|||||||||
12864|Mount Keith Granodiorite|32907|4|Described|p55|||Age dating||||||
12864|Mount Keith Granodiorite|35113|6|Mentioned|p32|||See also Fig.1, p40, p43.||||||31-JAN-08
12864|Mount Keith Granodiorite|37498|6|Mentioned|p367|||||||||
12864|Mount Keith Granodiorite|37795|6|Mentioned|Table 4|||||||||
12864|Mount Keith Granodiorite|38459|6|Mentioned|p1552|||||||||
12864|Mount Keith Granodiorite|38512|6|Mentioned|Table III|||||||||
12864|Mount Keith Granodiorite|38765|6|Mentioned|p100|||||||||
12864|Mount Keith Granodiorite|38979|6|Mentioned|p397|||||||||
12864|Mount Keith Granodiorite|40775|4|Described|p500|||||||||
12864|Mount Keith Granodiorite|71270|5|Briefly described|118936.1.pdf|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Sample GSWA 118936 (recrystallised granite) yielded a weighted mean 207Pb/206Pb age of 2685+\-7 Ma, interpreted to be the crystallisation age of the granite.|2685+\-7 Ma|||||
12871|Mount Kirk Formation|22682|5|Briefly described|Fig9,p14||Archean|||||||07-NOV-08
12871|Mount Kirk Formation|23136|6|Mentioned|p265 Fig.1|||||||||
12871|Mount Kirk Formation|23159|5|Briefly described|p790 fig4 table5|Archean|Archean|Spelt "Mt" in Fig4.||||||07-NOV-08
12871|Mount Kirk Formation|23786|5|Briefly described|p47|||Geological Province: Yilgarn Craton.||||||
12871|Mount Kirk Formation|23926|5|Briefly described|p9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
12871|Mount Kirk Formation|24165|5|Briefly described|p48|Archean|Archean|Mount Thirsty area. May be prospective for tantalum and tin.||||Is intruded by the Widgiemooltha dyke swarm.|Gabbro, pyroxenite, serpentinised peridotite, ferruginous chert, felsic volcanic rocks, and black shale.|
12871|Mount Kirk Formation|30562|4|Described|p7|||Archaean.||||||
12871|Mount Kirk Formation|30959|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
12871|Mount Kirk Formation|36869|6|Mentioned|p48|||||||||
12871|Mount Kirk Formation|41432|5|Briefly described|p13|||||||||
12871|Mount Kirk Formation|42195|6|Mentioned|p143|||||||||
12871|Mount Kirk Formation|42221|6|Mentioned|p33|||||||||
12871|Mount Kirk Formation|42785|5|Briefly described|Fig.7 P275|||Actually spelt Mt Kirk Formation.||||||
12871|Mount Kirk Formation|42937|5|Briefly described|p559|||actually spelt Mt Kirk Formation||||||
12871|Mount Kirk Formation|43102|5|Briefly described|p5|||||||||
12871|Mount Kirk Formation|43162|6|Mentioned|6, 9|||U-Pb Age: 2687+/-3Ma||||||
12871|Mount Kirk Formation|43498|5|Briefly described|2|||||||||
12871|Mount Kirk Formation|60076|5|Briefly described|p15|Archean|Archean|Tightly folded sequence of sedminetary rocks containing major gabbro sills.  Overlies Woolyeenyer Formation.  Age: 2714+/-5Ma.  Within the Norseman greenstones region.||||||07-NOV-08
12871|Mount Kirk Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Norseman Terrane. Kalgoorlie Sequence.|||||Felsic volcanic and volcaniclastic rocks.|
12871|Mount Kirk Formation|64633|6|Mentioned|p6 Fig.4.|||Kalgoorlie Terrane.||||Unconformably overlies Woolyeenyer Formation.|Volcaniclastic rocks: rhyolite/dacite provenance.|
12871|Mount Kirk Formation|66880|5|Briefly described|p8 Fig.2. |Archean|Archean|||||Unconformably overlies Woolyeenyer Formation.|Volcaniclastic rocks; rhyolite/dacite provenance.|
12871|Mount Kirk Formation|70326|5|Briefly described|p360,364|Neoarchean|Neoarchean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Underlain by Woolyeenyer Formation. Correlable to Black Flag Group and Vivien Metasediments.|Felsic, mafic to ultramafic rocks, including sediments.|
12871|Mount Kirk Formation|71212|6|Mentioned|p240, p241|||Norseman region.||||||
12871|Mount Kirk Formation|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Black Flag Group||||
12907|Mount Manning komatiite|40302|6|Mentioned|Table 1|||||||||
12923|Mount McGrath Formation|22484|5|Briefly described|p77 Fig.6|||||||||
12923|Mount McGrath Formation|23047|6|Mentioned|35|||Of the Wyloo Group. Hamersley Province. Underllain by Wyloo Group, Turee Creek Group, Hamersley Group and Fortescue Group.||||||10-FEB-09
12923|Mount McGrath Formation|23280|5|Briefly described|p1084,1086,Fig2p1086|||||||||
12923|Mount McGrath Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
12923|Mount McGrath Formation|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit Duck Creek Dolomite. Underlying unit Cheela Springs Basalt.||||||
12923|Mount McGrath Formation|23612|5|Briefly described|p841|Proterozoic|Archean|Of Wyloo Group.||||||07-NOV-08
12923|Mount McGrath Formation|23774|5|Briefly described|p733 table 1|||Age: 1843+/-2 Ma. Spelt 'Mt' in text. Of Wyloo Group.||||||
12923|Mount McGrath Formation|23890|6|Mentioned|p16|||||||||
12923|Mount McGrath Formation|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of Upper Wyloo Group. Unconformably overlies Wooly Dolomite. Conformably overlain by Duck Creek Dolomite. Deltaic and shallow marine cycles of ferruginous conglomerate and siltstone. Max. thickness: 1200 m. Geological Province: Ashburton Province.||||||07-NOV-08
12923|Mount McGrath Formation|24602|5|Briefly described|p853, p855 Fig. 2|||Of the Wyloo Group. Mount is Mt. in text. Geological Province: Ashburton Fold Belt.||||||
12923|Mount McGrath Formation|24607|4|Described|p967|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group. Unconformably overlies the Cheela Springs Basalt. Conformably overlain by the Duck Creek Dolomite. Detrital zircons give max depositional age: 2455 +/- 24 Ma. Geological Province: Ashburton Basin. Mount is Mt. in text.||||||30-NOV-10
12923|Mount McGrath Formation|33543|6|Mentioned|p132|||Refers de la Hunty (1965)||||||
12923|Mount McGrath Formation|34066|4|Described|p7||Proterozoic|Member of Wyloo Group.||||||
12923|Mount McGrath Formation|35260|6|Mentioned|p17|||||||||
12923|Mount McGrath Formation|35976|6|Mentioned|Fig.39|||See also Table 16.||||||
12923|Mount McGrath Formation|36551|6|Mentioned|Table 23|||||||||
12923|Mount McGrath Formation|36882|4|Described|p136|||||||||
12923|Mount McGrath Formation|36902|6|Mentioned|p15|||||||||
12923|Mount McGrath Formation|37327|6|Mentioned|p396|||||||||
12923|Mount McGrath Formation|37460|3|Fully described|p121|||||||||
12923|Mount McGrath Formation|38321|6|Mentioned|Table 1|||||||||
12923|Mount McGrath Formation|38482|6|Mentioned|p15|||||||||
12923|Mount McGrath Formation|38790|6|Mentioned|p165|||||||||
12923|Mount McGrath Formation|39210|5|Briefly described|Table 1|||||||||
12923|Mount McGrath Formation|40103|6|Mentioned|Fig.1|||||||||
12923|Mount McGrath Formation|40369|6|Mentioned|Plate 1|||||||||
12923|Mount McGrath Formation|40554|5|Briefly described|p29|||||||||
12923|Mount McGrath Formation|40905|6|Mentioned|Fig.1|||||||||
12923|Mount McGrath Formation|40937|6|Mentioned|p28|||||||||
12923|Mount McGrath Formation|41125|6|Mentioned|p28|||||||||
12923|Mount McGrath Formation|41845|6|Mentioned|Fig. 1|||||||||
12923|Mount McGrath Formation|41846|6|Mentioned|p94|||||||||
12923|Mount McGrath Formation|41955|6|Mentioned|Fig.1 P4|||||||||
12923|Mount McGrath Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
12923|Mount McGrath Formation|42148|6|Mentioned|p690|||||||||
12923|Mount McGrath Formation|42260|3|Fully described|p31|||||||||
12923|Mount McGrath Formation|42277|6|Mentioned|p55|||||||||
12923|Mount McGrath Formation|42435|6|Mentioned|Fig.1 P43|||||||||
12923|Mount McGrath Formation|42471|4|Described|p11|||||||||
12923|Mount McGrath Formation|42472|5|Briefly described|Map legend|||||||||
12923|Mount McGrath Formation|42686|5|Briefly described|map legend|Proterozoic||||||||
12923|Mount McGrath Formation|42704|5|Briefly described|Plate 2E|Proterozoic||Of the Wyloo Group.  Mudstone, sandstone, conglomerate, dolomite.||||||08-APR-09
12923|Mount McGrath Formation|42744|4|Described|p6|||||||||
12923|Mount McGrath Formation|43037|5|Briefly described|Fig.2,p24|||of Wyloo Group.  Actually spelt Mt. McGrath Formation||||||
12923|Mount McGrath Formation|43119|4|Described|p14|||of Wyloo Group||||||
12923|Mount McGrath Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Wyloo Group||||||
12923|Mount McGrath Formation|43290|4|Described|p9||Proterozoic|of Wyloo Group.||||||
12923|Mount McGrath Formation|43595|5|Briefly described|Table 3-8,p344||Paleoproterozoic|||||||07-NOV-08
12923|Mount McGrath Formation|44477|14|Not recorded|Table 1||Proterozoic|SF/50-6.||||||
12923|Mount McGrath Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
12923|Mount McGrath Formation|44481|5|Briefly described|map legend||Proterozoic|||||||
12923|Mount McGrath Formation|44692|4|Described|p.7,17,18,Tb.1, map|||O/lies Beasley River Quartzite; O/lain by Duck Creek Formation. (F50-11).||||||06-FEB-17
12923|Mount McGrath Formation|44729|5|Briefly described|map legend|Proterozoic||Of Wyloo Group||||||
12923|Mount McGrath Formation|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Of the upper part of the Wyloo Group.  Predominantly sandstone and siltstone.||||||07-NOV-08
12923|Mount McGrath Formation|61276|4|Described|p577-580|Paleoproterozoic|Orosirian|Overlies the Wooly Dolomite?unconformably. Post-iron ore mineralisation sedimentation. Krapez (1999) proposed min age of sedimentation, 1995 Ma. Figure shows max age ~1950 Ma. Must certainly be post-2008 Ma dykes that were eroded before Mt McGrath Fm deposition.|Age: younger than mafic dykes dated at 2008 Ma|Of the Wyloo Group||||17-OCT-16
12923|Mount McGrath Formation|61526|5|Briefly described|p880|||Of the Upper Wyloo Group. Clastics with some carbonates (stromatilitic in places) interbedded. Mount is Mt in text.||||||
12923|Mount McGrath Formation|62129|3|Fully described|p15, p20, p24|Proterozoic|Proterozoic|Of Wyloo Group. Discomformably underlain by Cheela Springs Basalt, conformably overlian by Duck Creek Dolomite. Thick: 1200m. Geol Prov: Ashburton Basin. Ferruginous conglomerate and sst, quartz sst, argillite, dolomitic argillite, and dolomite.||||||07-FEB-11
12923|Mount McGrath Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Metamorphosed ferruginous sandstone and conglomerate, pelite, and metadolomite.||||||
12923|Mount McGrath Formation|63866|5|Briefly described|p155|||A U-Pb SHRIMP xenotime age of 1738 +/- 5 Ma is given for gold mineralisation at the Mount Olympus deposit hosted in this formation (Sener et al., 2005).||||||
12923|Mount McGrath Formation|63869|5|Briefly described|p5-6|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.||Is overlain conformably by Duck Creek Dolomite.||
12923|Mount McGrath Formation|64384|5|Briefly described|p47 Tb. 7, p83|||Of Wyloo Group. Disconformable on Cheela Springs Basalt; conformable below Duck Creek Dolomite. Geological province: Ashburton Basin. Comprises ferruginous conglomerate and sandstone, + quartz sandstone, siltstone, mudstone and locally dev'd carbonate.||||||07-FEB-11
12923|Mount McGrath Formation|64728|6|Mentioned|p107.|||Contains detrital zircons with ages from c.3550 Ma to 2450 Ma.||Unit in lower Wyloo Group.||||
12923|Mount McGrath Formation|65830|6|Mentioned|p3|||||Of the Wyloo Group||||
12923|Mount McGrath Formation|66115|5|Briefly described|p136-138|Paleoproterozoic|Paleoproterozoic|||Wyloo Group||Is conformably overlain by (grades upwards into) Duck Creek Dolomite.|Black, tabular-bedded (~10 cm beds) siltstones grade upward into Duck Creek Dolomite.|
12923|Mount McGrath Formation|66574|5|Briefly described|p914 Fig.3, p928|||Base of upper Wyloo Group; overlies Wooly Dolomite of lower Wyloo Group. Fluvial conglomerate and sandstone.||||||
12923|Mount McGrath Formation|66950|6|Mentioned|p4, p4 Fig.3, p6|Rhyacian|Rhyacian|||Of the Wyloo Group.||||
12923|Mount McGrath Formation|67025|5|Briefly described|pp319-320, pp322-324, p328.|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.|||Includes hematite conglomerate.|
12923|Mount McGrath Formation|67056|4|Described|p419 Fig.2, p437.|Paleoproterozoic|Paleoproterozoic|Contains sporadic high-grade martite-microplaty hematite ore fragments and concentrations, eg the Barrett-Lennard detrital deposits (c.2 Mt). The age of the base of this unit is in dispute.|c.1850 Ma.|Basal unit in Upper Wyloo Group.||Unconformably overlies Lower Wyloo Group. Is overlain by Duck Creek Dolomite.||14-MAR-12
12923|Mount McGrath Formation|67130|5|Briefly described|p3 fig 2, p5, p24 fig 17|Siderian|Siderian|Up to 900m thick. Interpreted as upward fining deltaic and shallow marine cycles. Also spelled Mount McGrath Formation (p5)|2455 Ma +/- 12 Ma|Wyloo Group, Upper||Unconformably overlies Wooly Dolomite, Wyloo Group, Lower,  conformably overlain by Duck Creek Dolomite|Ferruginous conglomerate and sandstone, quartz sandstone, siltstone, mudstone and carbonate.|
12923|Mount McGrath Formation|67721|5|Briefly described|p37, p38 Fig.9|Paleoproterozoic|Paleoproterozoic|Approximately 40 m thick.|c. 2553 Ma|Of the upper Wyloo Group.||||
12923|Mount McGrath Formation|67827|5|Briefly described|p416-417, p426-429|Orosirian|Orosirian|South of Wyloo Dome. Hematite-pebble concentrations include the c.2 million tonnes Barrett-Lennard deposit.|c.1.85 Ga.|Basal unit in Upper Wyloo Group.||Is overlain by Duck Creek Dolomite.|Basal conglomerates contain hematite-pebble concentrations.|
12923|Mount McGrath Formation|67829|5|Briefly described|p451.|||Contains detrital, hematite-rich iron ore-bearing conglomerates. Occurs at the base of the upper Wyloo Group.||Unit in Wyloo Group.||||
12923|Mount McGrath Formation|67855|4|Described|p212 fig 3-10, p214-p215, p228, 231|Paleoproterozoic|Paleoproterozoic|Up to 1200m thick thinning to zero western margin of Wyloo Dome. 5 facies are described: Distributary-channel (clast supported conglomerate); Interdistributary-bay (ferruginous siltstone and mudstone intercalated with granule to fine-pebble conglomerate and sandstone); Distributary-mouth-bar (quartz sandstone; minor mudstone and siltstone); Shoreface and beach (quartz sandstone with mudstone clasts); Prodelta (mudstone and thin laminated siltstone and sandstone).||Of Wyloo Group||Overlain by Duck Creek Dolomite (conformably). Overlies Wooly Dolomite, Cheela Springs Basalt (unconformably/disconformably).|Ferruginous conglomerate and sandstone, quartz sandstone, siltstone, mudstone and local carbonate.|
12923|Mount McGrath Formation|68035|5|Briefly described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|<2455+/- 12 Ma det[rital zircon?]|Of upper Wyloo Group.||Unconformably overlies folded lower Wyloo Group and older rocks. Conformably overlain by Duck Creek Dolomite.|Upward-fining deltaic and shallow-marine cycles composed of channelized conglomerate and siltstone.|
12923|Mount McGrath Formation|69003|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Ashburton Basin, Capricorn Orogen.||Basal upper Wyloo Group.||Unconformably overlies lower Wyloo Group. Is overlain ?conformably by Duck Creek Dolomite.|Fluvial to shallow-marine sandstone and mudstone.|
12923|Mount McGrath Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. Mapped with Duck Creek Dolomite 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
12923|Mount McGrath Formation|69080|6|Mentioned|p687, p694|||||Unit in Wyloo Group.||Is overlain by Duck Creek Dolomite.||
12923|Mount McGrath Formation|69538|5|Briefly described|p517 Fig.3, p522 Fig.5, p533|Paleoproterozoic|Paleoproterozoic|Earliest known Hamersley Province hematite detritals. Hosts the ~2 Mt Barrett-Lennard detrital iron deposit.|~1.85 Ga.|Unit in Wyloo Group.|||Fluvio-deltaic: sporadic accumulations and mixed BIF and M-mplH ore fragments.|26-MAY-16
12923|Mount McGrath Formation|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.||Wyloo Group.||Overlies Cheela Springs Basalt.||
12923|Mount McGrath Formation|69596|6|Mentioned|p6|||Pilbara Craton.||||||
12923|Mount McGrath Formation|69745|6|Mentioned|p270-271, 273, 275-276, 286-287, 289|||Hamersley Province.||Upper Wyloo Group.||Is overlain by June Hill volcanics.|Basal conglomerates with pebbles of predominantly white chert and lesser mafic (volcanic) and shaly clasts. Hematite conglomerates, characteristic elsewhere in the Province, were not encountered in the Mt. Wall area.|
12923|Mount McGrath Formation|70086|5|Briefly described|p196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Wyloo Group.||Uppermost unit of the Wyloo Group. Underlain by Cheela Springs Basalt.||
12923|Mount McGrath Formation|70327|5|Briefly described|p2, p7-8, p10-13, p15-16|||McGrath Basin. Appears as Mt McGrath Formation. Dolostones at Urandy Creek Outcamp, and shales and dolostones E of Red Hill, assigned to this unit by Thorne and Seymour (1991), are here designated as Wooly Dolomite.||||Unconformably overlies Beasley River Quartzite, Cheela Springs Basalt and Wooly Dolomite. Is overlain by Duck Creek Dolomite.|Includes sandstone, black and red shales.|
12923|Mount McGrath Formation|70949|5|Briefly described|p987-989|Paleoproterozoic|Paleoproterozoic|Northern Capricorn Orogen. Hosts the Paulsens Mine gold deposit.||Wyloo Group.|||Includes low-grade metasediments: ferruginous epiclastic sedimentary rocks.|
12923|Mount McGrath Formation|70958|4|Described|p4-5, p14 App. 1, p16, Fig. 1|Paleoproterozoic|Paleoproterozoic|Usage restricted to the essentially clastic rocks that overlie, disconformably the Cheela Springs Basalt. Siad to be defined but no type section given. At Beasley River, 800m thick. Estimated to be up to 4km thick at Snowy Mountain.||Of Wyloo Group|In SW corner of Mount Bruce map sheet area, includes? Coolbye Shale Member, Karlathundra Conglomerate Member of de la Hunty (1965).|Disconformably overlies Cheela Springs Basalt. Overlaps older units (eg Hamersley Group) unconformably. Mainly overlain conformably by Duck Creek Dolomite, but some interfingering.|Predominantly coarse and fine clastics including quartzites and phyllitic siltstones and shales, with conglomerates at the base. Some carbonate lenses.|
12923|Mount McGrath Formation|71112|5|Briefly described|p69-70,75,79|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton.||||Underlain unconformably by Wooly Dolomite.|Deltaic siliciclastic sandstones and shales.|
12923|Mount McGrath Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, crystalline dolostone/dolomite, sandstone, siltstone|
12923|Mount McGrath Formation|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|c.2008 Ma.|Wyloo Group.|||Ferruginous sandstone, conglomerate and pebbly sandstone; quartz sandstone, siltstone, dolomitic siltstone, and dolostone.|
12923|Mount McGrath Formation|71808|6|Mentioned|p50, p149, p156|||||Wyloo Group, Upper||||
12923|Mount McGrath Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.||Wyloo Group|||Ferruginous sandstone, conglomerate and pebbly sandstone; quartz sandstone, siltstone, dolomitic siltstone, and dolostone.|
12923|Mount McGrath Formation|72570|6|Mentioned|p3 fig 1|||||Wyloo Group||||
12923|Mount McGrath Formation|72712|5|Briefly described|p5, p9, p25, p31, p33-34, 42-p43.|Orosirian|Orosirian|Revised here to be in an equivalent stratigraphic position to only the Karlathundra Conglomerate Member of Halligan and Daniels (1964). In part equivalent to old Mount McGrath Beds. Included the Coolbye Shale Member (Halligan and Daniels (1964). See also p45, p53.||Wyloo Group|Includes Karlathundra Conglomerate Member?|Unconformably overlies Wooly Formation. Conformably overlain by Duck Creek Dolomite.|Predominantly of medium- to coarse-grained siliciclastic rocks and minor argillite.|14-JAN-21
12923|Mount McGrath Formation|72758|4|Described|p13 Tb.1, p31-32, p34-35, p42, p45.|Paleoproterozoic|Paleoproterozoic|Up to 900 m thick. Predominantly deltaic and shallow-marine shelf deposits. See also p40, p47, p57.||Wyloo Group||Unconformably overlies Wooly Dolomite and disconformably overlies Cheela Springs Basalt and conformably underlies Duck Creek Dolomite.|Includes ferruginous conglomerate, arenite, wacke, mudstone, dolomitic mudstone, dolomite.|
12926|Mount McRae Shale|22682|5|Briefly described|p29|||Overlies Mount Sylvia Formation||||||
12926|Mount McRae Shale|22689|6|Mentioned|Fig. 1 p138|||Of Hamersley Group.||||||
12926|Mount McRae Shale|22701|5|Briefly described|Fig2,p39|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin. Overlies Mount Sylvia Formation. Overlain by Brockman Iron Formation.||||||07-NOV-08
12926|Mount McRae Shale|23045|5|Briefly described|289|||Parent Hamersley Group||||||
12926|Mount McRae Shale|23046|6|Mentioned|184|||Overlying unit Dales Gorge Member||||||
12926|Mount McRae Shale|23126|5|Briefly described|p383 Fig.3|||||||||
12926|Mount McRae Shale|23127|5|Briefly described|p376|||||||||
12926|Mount McRae Shale|23536|5|Briefly described|Fig 2 p 429|||||||||
12926|Mount McRae Shale|23575|5|Briefly described|Map Legend|Proterozoic|Archean|Of Hamersley Group||||||07-NOV-08
12926|Mount McRae Shale|23612|5|Briefly described|p843|||||||||
12926|Mount McRae Shale|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
12926|Mount McRae Shale|24041|6|Mentioned|p492|||Mount is Mt in text||||||
12926|Mount McRae Shale|24426|4|Described|p218, 220|Paleoproterozoic|Archean|Written Mt in text. Thickness: ~100 m. Thinly bedded black shale, chert carbonates and cherty banded iron-formation. Overlies Mount Sylvia Formation. Overlain by Brockman Iron Formation. Geological Province: Hamersley Province.||||||07-FEB-11
12926|Mount McRae Shale|24544|4|Described|p57 Fig.43|Paleoproterozoic|Archean|Of Hamersley Group. Overlies Mount Sylvia Formation. Overlain by Brockman Iron Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
12926|Mount McRae Shale|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Mount is spelt Mt. in text. Geological Province: Pilbara Craton||||||
12926|Mount McRae Shale|29595|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|29629|6|Mentioned|p900|||||||||
12926|Mount McRae Shale|30685|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|31021|5|Briefly described|p893|||||||||
12926|Mount McRae Shale|31670|4|Described|p911|||||||||
12926|Mount McRae Shale|31671|5|Briefly described|p11|||||||||
12926|Mount McRae Shale|31828|6|Mentioned|p40|||Stratigraphic table||||||
12926|Mount McRae Shale|32326|6|Mentioned|p122|||Hamersley Gp.||||||
12926|Mount McRae Shale|33538|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|33540|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|33542|6|Mentioned|p412|||||||||
12926|Mount McRae Shale|33544|2|Defined|p86|Precambrian|Precambrian|See also PP87 - 89||||||
12926|Mount McRae Shale|33687|5|Briefly described|p917|||||||||
12926|Mount McRae Shale|34023|6|Mentioned|p46|||||||||
12926|Mount McRae Shale|34066|4|Described|p5|||L.Prot.||||||
12926|Mount McRae Shale|34135|5|Briefly described|Table 2|||See also P16.||||||
12926|Mount McRae Shale|35052|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|35260|6|Mentioned|Fig.4|||||||||
12926|Mount McRae Shale|35299|5|Briefly described|p893|||||||||
12926|Mount McRae Shale|35976|6|Mentioned|Fig.39|||||||||
12926|Mount McRae Shale|36091|5|Briefly described|p572|||||||||
12926|Mount McRae Shale|36247|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|36551|6|Mentioned|Table 23|||||||||
12926|Mount McRae Shale|36642|6|Mentioned|Table 1|||||||||
12926|Mount McRae Shale|36882|4|Described|p134|||||||||
12926|Mount McRae Shale|37297|6|Mentioned|Fig.2|||||||||
12926|Mount McRae Shale|37460|6|Mentioned|Fig.3.4|||||||||
12926|Mount McRae Shale|37704|6|Mentioned|Fig.1|||||||||
12926|Mount McRae Shale|37708|6|Mentioned|p1930|||||||||
12926|Mount McRae Shale|38790|6|Mentioned|p164|||||||||
12926|Mount McRae Shale|39200|4|Described|p285|||||||||
12926|Mount McRae Shale|39210|5|Briefly described|Table 1|||||||||
12926|Mount McRae Shale|39697|5|Briefly described|p126|||||||||
12926|Mount McRae Shale|40369|6|Mentioned|Plate 1|||||||||
12926|Mount McRae Shale|40987|6|Mentioned|Fig.3|||||||||
12926|Mount McRae Shale|41358|5|Briefly described|p145|||||||||
12926|Mount McRae Shale|41768|5|Briefly described|Table 1|||See also P28||||||
12926|Mount McRae Shale|42013|5|Briefly described|Map legend|Archean||||||||07-NOV-08
12926|Mount McRae Shale|42112|5|Briefly described|p9|||||||||
12926|Mount McRae Shale|42190|6|Mentioned|p278|||||||||
12926|Mount McRae Shale|42471|5|Briefly described|p7|||||||||
12926|Mount McRae Shale|42472|5|Briefly described|Map legend|||||||||
12926|Mount McRae Shale|42495|5|Briefly described|p35|||||||||
12926|Mount McRae Shale|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
12926|Mount McRae Shale|42704|5|Briefly described|Plate 2E|Proterozoic|Archean|Of the Hamersley group. grouped with Mount Sylvia Formation and Wittenoom Dolomite in map legend.||||||07-NOV-08
12926|Mount McRae Shale|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
12926|Mount McRae Shale|42744|5|Briefly described|p5|||||||||
12926|Mount McRae Shale|43064|5|Briefly described|Fig.2,p70|||||||||
12926|Mount McRae Shale|43119|5|Briefly described|p10|||of Hamersley Group||||||
12926|Mount McRae Shale|43210|5|Briefly described|Table 1 p3,p4.||Paleoproterozoic|of Hamersley Group.||||||07-NOV-08
12926|Mount McRae Shale|43262|5|Briefly described|Map Legend||Archean|of Hamersley Group.||||||07-NOV-08
12926|Mount McRae Shale|43290|5|Briefly described|p6||Archean|of Hamersley Group.||||||07-NOV-08
12926|Mount McRae Shale|43595|6|Mentioned|Fig.2-49,p220|||||||||
12926|Mount McRae Shale|44152|5|Briefly described|p178, p179 Fig.2-155|||The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Hamersley Group||Overlies Mount Sylvia Formation. Is overlain by Dales Gorge Member (Brockman Iron Formation).|Shale, thin bands of shard-bearing volcanic ash in upper parts.|
12926|Mount McRae Shale|44477|4|Described|p.10, Table 1||Proterozoic|SF/50-6.||||||
12926|Mount McRae Shale|44478|14|Not recorded|map legend||Proterozoic|||||||
12926|Mount McRae Shale|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
12926|Mount McRae Shale|44501|14|Not recorded|p.6,18, table 4, map||Paleoproterozoic|(ref. to MacLeod et al 1963). (F/50-7). Lower Proterzoic.||||||07-NOV-08
12926|Mount McRae Shale|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
12926|Mount McRae Shale|44503|2|Defined|p.14, Tb.2, map|||Roy Hill Sheet. (F50-12).||||||
12926|Mount McRae Shale|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
12926|Mount McRae Shale|44692|2|Defined|p.7,13,15,Tb.1, map|||Conf.o/lies Mt. Sylvia Formation. O/lain by Brockman Iron Formation. (F50-11).||||||
12926|Mount McRae Shale|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
12926|Mount McRae Shale|50227|5|Briefly described|p443 Fig. 1|||Conformably overlain by Dales Gorge Member.||||||07-FEB-11
12926|Mount McRae Shale|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersley Group. Overlian by Mount McRae Shale, underlain by Wittenoom Formation.||||||20-MAR-12
12926|Mount McRae Shale|60706|5|Briefly described|p623 Fig.2|||Of the Hamersley Group. Geological Province: Hamersley Basin. Mount is Mt in text of figure.||||||
12926|Mount McRae Shale|61265|6|Mentioned|p46-47 Fig.2|||Geological Province: Pilbara Craton.||||||
12926|Mount McRae Shale|61268|5|Briefly described|p79, p78 Tb.1|||Of the Hamersley Group. Mudstone, siltstone, chert, iron-formation, and dolomite. See also p80 Fig.2||||||
12926|Mount McRae Shale|61575|5|Briefly described|p760 Fig. 2|||Mount is Mt in text of figure.||||||
12926|Mount McRae Shale|61576|5|Briefly described|p774 Fig. 1|||Of the Hamersley Group. Geological Province: Hamersley Basin.||||||
12926|Mount McRae Shale|62129|3|Fully described|p9-10|Archaean|Archaean|Of Hamersley Group. Thickness: 70m. Geological Province: Hamersley Basin. Interlayered shale, dolomitic shale, chert, and minor BIF.||||||07-FEB-11
12926|Mount McRae Shale|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
12926|Mount McRae Shale|63153|6|Mentioned|p1360, p1362 Fig.3. |||Shows tighter, almost convoluted, folding. Appears as Mt McRae Formation in Fig.4.||Unit in Hamersley Group.||Overlies Mount Sylvia Formation. Is overlain by Brockman Iron Formation.||
12926|Mount McRae Shale|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
12926|Mount McRae Shale|63432|5|Briefly described|p736 Fig. 2|Proterozoic|Proterozoic|Mount is Mt in text of figure.||||||07-FEB-11
12926|Mount McRae Shale|64384|5|Briefly described|p35 Tb. 6, p56|||Of the Hamersley Group. Geological province: Hamersley Basin. Comprises interlayered shales (some graphitic), cherts and BIF; upper part hosts iron ore.||||||07-FEB-11
12926|Mount McRae Shale|64580|4|Described|map legend|Paleoproterozoic|Neoarchean|Of Hamersley Group. Mudstone, siltstone, chert, banded iron-formation, and dolomite; metamorphosed.||||||09-DEC-08
12926|Mount McRae Shale|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Geological Province: Hamersley Basin. Shale, dolomitic shale, chert, and minor banded iron-formation.||||||
12926|Mount McRae Shale|64724|5|Briefly described|p42 Fig. 3|Paleoproterozoic|Neoarchean|||Of Hamersley Group.||||02-APR-12
12926|Mount McRae Shale|64725|6|Mentioned|p58.|||||Unit in Hamersley Group.||Overlies Mount Silvia Formation. Is overlain by Brockman Iron-formation.||
12926|Mount McRae Shale|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.||||||
12926|Mount McRae Shale|65683|5|Briefly described|p801 Fig2|||Of Hamersley Group. Underlies Dales Gorge Member of the Brockman Iron Formation; overlies Mount Sylvia Formation.||||||08-MAR-12
12926|Mount McRae Shale|67025|4|Described|pp318-320, p322 Table 3, pp324-326.|||||Unit in Hamersley Group.||Conformably overlies Mount Sylvia Formation. Is overlain conformably by Brockman Iron Formation.|Shale, dolomite.|
12926|Mount McRae Shale|67056|4|Described|p419 Fig.2, pp441-442, p447.|||The upper parts of this unit contain abundant fine reactive pyrite and hydrocarbons. This may have allowed exothermic oxidation reactions to generate post-ore convective hydrothermal cells which would have produced the observed metasomatism.||Unit in Hamersley Group.|Includes Colonial Chert Member.|Overlies Bruno's Band. Is overlain by Brockman Iron Formation.|Carbonate turbidites common.|
12926|Mount McRae Shale|67130|5|Briefly described|p3 fig 2, p24 fig 17, p34 fig 29|Siderian|Neoarchean||2501 +/- 8 Ma|Hamersley Group||Overlies Mount Sylvia Formation, Overlain by Brockman Iron Formation|Shale|
12926|Mount McRae Shale|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Hamersley Group||||
12926|Mount McRae Shale|67201|4|Described|p34, p51-53|||Visible at base of Hamersley Range Escarpment, overlying Mount Sylvia Formation. Thickness: 70 m.||Hamersley Group||Overlies Mount Sylvia Formation, and is overlain by Brockman Iron Formation.|Alternating shale, dolomitic shale, chert and minor BIF.|24-NOV-16
12926|Mount McRae Shale|67721|6|Mentioned|p38 Fig.9|||Pyrite zone in middle (nodules, blebs)||Of the Hamersley Group.||||
12926|Mount McRae Shale|67855|5|Briefly described|p226, 227||||||||Alternations of thin-bedded shale, siltstone, chert and baneded iron-elastica formation.|
12926|Mount McRae Shale|68035|5|Briefly described|p292 Fig 6, p293|Paleoproterozoic|Neoarchean|Hamersley Basin.|2501 +/-8 Ma.|Of Hamersley Group.||Overlies Mount Sylvia Formation,overlain by Brockman Iron Formation.|Shale.|
12926|Mount McRae Shale|68280|5|Briefly described|p5, p41, p54|Neoarchean|Neoarchean||2560-2500 Ma|Hamersley Group||Overlain by Brockman Iron Formation, overlies Mount Sylvia Formation|Shale.|
12926|Mount McRae Shale|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Hamersley Basin. Mapped with Mount Sylvia Formation as a single unit.||Of the Hamersley Group.|||Mudstone, siltstone, chert, banded iron-formation and dolomite; metamorphosed.|06-MAY-14
12926|Mount McRae Shale|69080|6|Mentioned|p687|||||Unit in Hamersley Group.||Overlies Mount Sylvia Formation. Is overlain by Brockman Iron Formation.||
12926|Mount McRae Shale|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Shale, dolomitic shale, chert, and minor banded iron-formation|
12926|Mount McRae Shale|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|
12926|Mount McRae Shale|69538|5|Briefly described|p517 Fig.3, p523, p525, p528-529|Paleoproterozoic|Paleoproterozoic|See also p531 Fig.11, p532 Tb.3, p551 Fig.27, p564 Fig.37, p570-571, p574-575, p578 Fig.47, p583-585. Highly detailed discussion of formation of detrital iron ore deposits.||Unit in Hamersley Group.||Overlies Mount Sylvia Formation. Is overlain by Dales Gorge Member.||
12926|Mount McRae Shale|69543|6|Mentioned|p97|||Sulfur isotope ratios in the lower unit of this formation are similar to those in Meteorite Bore Member (Turee Creek Group), suggesting this formation was a source of pyrite grains in the latter.|~2.50 Ga.|||||
12926|Mount McRae Shale|69563|5|Briefly described|p689-691, p693, p696 Fig.6, p698-699|||Contains tsunami-related deposits [?post-asteroid impact] at the top of the unit.|2501 +/- 8 Ma.|||Underlies Dales Gorge Member.||
12926|Mount McRae Shale|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|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.|2501 Ma (isotopic)|Unit of Hamersley Group.|||Shale, dolomitic shale, chert, and minor banded iron-formation|
12926|Mount McRae Shale|69739|6|Mentioned|p69-72|||Hamersley Basin.||||Overlies Mount Sylvia Formation. Is overlain by Brockman Iron Formation.|Chloritic, carbonaceous and pyritic shales.|
12926|Mount McRae Shale|69745|6|Mentioned|p278-279, 281-282, 290|||Mount Wall area, Hamersley Province. See also references to Mount McRae Formation (p272-273, 287) and McRae Shale Formation (p277, 284).||||||
12926|Mount McRae Shale|69989|6|Mentioned|p33|Archean|Archean|Variations in S isotope ratios may reflect temporal changes in atmospheric chemistry.||||||
12926|Mount McRae Shale|70509|5|Briefly described|p14,33|Neoarchean|Neoarchean|Geological province: Hamersley Province; Pilbara Craton.|2501+\-8 Ma|Unit of Hamersley Group.||Overlain by Brockman Iron Formation/Dales Gorge Member. Underlain by Wittenoom Dolomite.||
12926|Mount McRae Shale|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2541-2501 Ma||||Mudstone, siltstone, chert, banded iron formation and metamorphosed dolomite.|
12926|Mount McRae Shale|70826|6|Mentioned|p8|Proterozoic|Neoarchean|||Hamersley Group, lower||||
12926|Mount McRae Shale|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|Oakover Basin.||Hamersley Group||||
12926|Mount McRae Shale|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||shale, chert, banded iron formation|
12926|Mount McRae Shale|71785|6|Mentioned|p88|||||||||
12926|Mount McRae Shale|71808|4|Described|vii, p6, p23, p26-p27|||Hamersley Province. Subdivided into four facies in the present study: Carbonate-massive chert facies, Anoxic facies, carbonate turbidite facies and colonial chert member. Exposure is typically poor, being covered by a scree slope derived from the Dales Gorge Member and as such outcrop is poorly described. Extensive exposures are however described from the northern side of the Hamersley Province. See also See also p30, p51, p71, p101, p102, p117, p132-p133, p135, p149-p150, p156, p185-p186, p188-p189, p192, p230, p241.||Hamersley Group||Overlain by the Brockman Iron Formation.|Carbonates, chert, carbonaceous shale, turbiditic rocks, banded iron formation.|
12926|Mount McRae Shale|72034|6|Mentioned|500k_interpgeop16_lut|Neoarchean|Neoarchean|Hamersley Basin.  Shown as a combined informal unit with Mount McRae Shale.||Hamersley Group, lower||||
12926|Mount McRae Shale|72493|5|Briefly described|p29-30|Archaean|Archaean|Hamersley Basin. On p29 is referred to as Mount McRae Member.|2501 +/- 8 Ma.|Hamersley Group.||Overlies Mount Sylvia Formation. Is overlain by Dales Gorge Member (Brockman Iron Formation).||
12926|Mount McRae Shale|72569|6|Mentioned|p5|||Of the Hamersley Basin.||||||
12926|Mount McRae Shale|72570|6|Mentioned|p3 fig 1|||||Hamersley Group||||
12926|Mount McRae Shale|72712|5|Briefly described|p3, p10, p7 Fig.4, p9 Fig.5, p11 Fig.8.|Paleoproterozoic|Neoarchean|Interpreted recently by Martin et al. (2000) and Martin and Morris (2010).|c. 2565 Ma to c. 2495 Ma.|Hamersley Group||Overlies Mount Sylvia Formation. Underlies Brockman Iron Formation.|Includes shales.|
12926|Mount McRae Shale|72758|5|Briefly described|p15 Tb.1, p24-25.|||90m thick sequence in Wyloo mapsheet area. A 4m thick chert forms a prominent marker bed near the middle of the formation in the northeastern part of Wyloo. Misspelt as Mount McCrae Shale p23.||Hamersley Group||Conformably overlies Mount Sylvia Formation. Conformably overlain by Brockman Iron Formation.|Includes thin-bedded, laminated mudstone containing small amounts of chert, dolomite, and BIF, which become more abundant towards the top of the formation.|
12926|Mount McRae Shale|73022|4|Described|p2-3, p4 Fig.3, p7 Fig.9|||Siliciclastic and carbonate beds represent distal turbidites and hemi-pelagites deposited on a deep-water shelf floored by continental crust. Some ferruginous chert beds contain greenalite nanoparticles, syneresis structures and shrinkage structures indicting a depositional origin from hydrothermal vent plumes.|2.50 Ga|Hamersley Group|Colonial Chert Member|Overlies the Mount Sylvia Formation, underlies the Colonial Chert Member.|Fine-grained siliciclastic and carbonate beds comprising shale, minor Fe-chert and banded iron formation, intercalated with regional chert bands including laminated chert.|
12926|Mount McRae Shale|73290|6|Mentioned|p784|||Hamersley Province.||||||
12953|Mount Murchison Quartzite|41261|6|Mentioned|p16|||||||||
12961|Mount Narryer quartzite|23785|5|Briefly described|p18|Archean|Archean|Informal name. Geological Province: Yilgarn Craton.||||||07-NOV-08
12961|Mount Narryer quartzite|41333|5|Briefly described|p338|||||||||
12961|Mount Narryer quartzite|41942|5|Briefly described|p53|||||||||
12961|Mount Narryer quartzite|50128|5|Briefly described|p42|Archean|Archean|Depositional age: ca 3100 Ma. Geological Province: Yilgarn Craton. Mount is Mt. in text.||||||07-NOV-08
12967|Mount Negri Volcanics|22471|5|Briefly described|27|Archean|Archean|Geol province Pilbara||||||07-NOV-08
12967|Mount Negri Volcanics|22715|5|Briefly described|table7, fig7|Archean|Archean|Age: 2920Ma. Spelt "Mt" in Figure 7.||||||07-NOV-08
12967|Mount Negri Volcanics|23244|5|Briefly described|Fig.2,5 p22|||of Whim Creek Belt. Underlying unit Louden Volcanics.||||||
12967|Mount Negri Volcanics|23348|5|Briefly described|220|||||||||
12967|Mount Negri Volcanics|23598|4|Described|p12|||Defined by Hickman 1990. Underlain by Louden Volcanics.||||||21-AUG-07
12967|Mount Negri Volcanics|23743|6|Mentioned|p3|||Geological Province: Pilbara Craton.||||||
12967|Mount Negri Volcanics|23784|5|Briefly described|p20|Archean|Archean|Of Bookingarra Group.||||||07-NOV-08
12967|Mount Negri Volcanics|23789|5|Briefly described|p24|||See also Negri Volcanics.||||||
12967|Mount Negri Volcanics|23793|4|Described|p27|Archean|Archean|Of Bookingarra Group. Formerly Negri Volcanics.||||||07-NOV-08
12967|Mount Negri Volcanics|23794|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province Pilbara Craton.||||||07-NOV-08
12967|Mount Negri 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
12967|Mount Negri Volcanics|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.3.0-2.925 Ga. Geological Province: Pilbara Craton. Overlying Unit: Louden Volcanics.||||||07-NOV-08
12967|Mount Negri Volcanics|24023|5|Briefly described|p18|||||||||
12967|Mount Negri Volcanics|24140|5|Briefly described|p217 Fig. 2|Archean|Archean|Supersedes Negri Volcanics and Louden Volcanics.  Basaltic sheet lava, pillow lava and breccia.||||||07-NOV-08
12967|Mount Negri Volcanics|24169|5|Briefly described|p666 Fig. 5|||Mount is Mt. in text.||||||
12967|Mount Negri Volcanics|24184|4|Described|p714, p716 Fig.12|Archean|Archean|Of the Bookingarra Group. 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
12967|Mount Negri Volcanics|24185|5|Briefly described|p746 Tb.4|Archean|Archean|Mount is Mt. in text. Geological Province: Pilbara Craton.||||||07-NOV-08
12967|Mount Negri Volcanics|24191|4|Described|p830 Fig. 2, p831|Archean|Archean|Of Bookingarra Group.  Comprises subaerial and subaqeous basalt sheet lava.  Geological Province: Pilbara Craton.||||||07-NOV-08
12967|Mount Negri Volcanics|24550|6|Mentioned|p39|||Same as Negri Volcanics? Probably misspelt? Predominantly mafic rocks.||||||07-FEB-11
12967|Mount Negri Volcanics|30766|6|Mentioned|p18|||Refers Miller & Gain||||||
12967|Mount Negri Volcanics|43052|5|Briefly described|Fig.3.8|||actually spelt Mt Negri Volcanics||||||
12967|Mount Negri Volcanics|43698|6|Mentioned|p18|||||||||
12967|Mount Negri Volcanics|43821|5|Briefly described|map legend|Archean|Archean|Of Pilbara Supergroup||||||07-NOV-08
12967|Mount Negri Volcanics|44150|5|Briefly described|p132 Fig.2-131, p137|||Usually flat-lying.||Pilbara Supergroup||Overlies Louden Volcanics unconformably. Is overlain unconformably by Mount Roe Basalt (Fortescue Group).|Suite of tholeiitic to andesite lavas.|
12967|Mount Negri Volcanics|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
12967|Mount Negri Volcanics|60362|5|Briefly described|p1517-1529, |Archean|Archean|NW Mallina Basin. Geochemistry detailed and tabulated.||Bookingarra Group.|||Subaqueous flows of siliceous high-Mg basalt. Vesicular flows common.|
12967|Mount Negri Volcanics|61267|6|Mentioned|p72 fig.1|||Geological Province: Pilbara Craton||||||
12967|Mount Negri Volcanics|63372|4|Described|Map Legend|Archean|Archean|Of the Bookingarra Group. Geological Province: Whim Creek and Mallina Basin. Age: 2975-2945Ma. Variolitic and vesicular basalt, undivided; metamorphosed.||||||07-NOV-08
12967|Mount Negri Volcanics|63441|4|Described|p6 Tb. 1, p27|Archean|Archean|Formerly of Bookingarra Gp; now redefined as Mt Negri Volcanic Member of Bookingara Fm.(Croydon Gp, De Grey Supergp). Overlies Cistern Fm. Weakly metamorph'd basaltic succession of variolitic basalt+vesicular basalt, with local pyroxene-spinifex textures||||||07-FEB-11
12967|Mount Negri Volcanics|63538|4|Described|p7, p32, p33, p34, p35|Archean|Archean|Of Bookingarra Formation. Underlain by Croyden Group. Geological Province: Pilbara Craton. Typically vesicular flow units with interlayered hyaloclastite deposits.||||||19-APR-13
12967|Mount Negri Volcanics|65415|4|Described|p119 Fig.1, p120 Fig.2, p121.|Archean|Archean|Hickman (1990); formerly Negri Volcanics (Hickman 1983). High TiO2 compared with Louden Volcanics.||Unit in Pilbara Supergroup.||Unconformably overlies Louden Volcanics. Is overlain unconformably by Mount Bruce Supergroup.|Variolitic-textured basalts.|
12967|Mount Negri Volcanics|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv||Archean|Geological province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin.||||||
12967|Mount Negri Volcanics|69299|5|Briefly described|p6 Tb.1|Archean|Archean|Thickness on COOYA POOYA: 0-1000 m.||Of Bookingarra Group.|||Variolitic and vesicular basalt.|
12967|Mount Negri Volcanics|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.||Bookingarra Group|Comstock Member||metamorphosed variolitic and vesicular basalt, undivided|
12967|Mount Negri Volcanics|70775|4|Described|p12, p24, p29 tbl 5,  p95-p96|Mesoarchean|Mesoarchean|Mallina Basin. Name is derived from Mount Negri which is also the location of the type area. An age of 2950 Ma is also given by Smithies et al., 2004a. Previously used as an informal name of Miller and Gair (1975) and rocks belonging to this formation and the Louden Volcanics were included within the 'Negri Volcanics' of Fitton et al (1975). That name was first formally defined by the Hickman (1983) to refer only to the unit later renamed as the Mount Negri Volcanics (Hickman, 1990). The Mount Negri Volcanics were recently renamed, but not formally redefined as the Mount Negri Volcanic Member by Van Kranendonk et al., 2006 [NB the current authors propose to continue using Mount Negri Volcanics and redefine it on p97]. Up to 500m thick (maximum stratigraphic thickness) but generally between 100 and 200m in most areas. See also p41, p45-p46, p51, p54-p56, p60-p61, p63.|c. 2950 Ma (Arndt et al, 2001)|Bookingarra Group||Unconformably overlies the Rushall Slate, Cistern Formation and the Louden Volcanics. Overlain by the Mallina Formation (upper).|Variolitic and vesicular tholeiitic basalts and komatiitic basalts and komatiites.|17-MAY-21
12967|Mount Negri Volcanics|72251|5|Briefly described|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton.||||Contemporaneous with Sisters Supersuite.||
12980|Mount North Lamproite|41158|6|Mentioned|Table 31|||||||||
13010|Mount Parker Sandstone|22440|5|Briefly described|p4,5|Stenian|Stenian|Age 1200- 1000Ma.||||||09-NOV-06
13010|Mount Parker Sandstone|22496|6|Mentioned|p10||Neoproterozoic|Superseded by Mount Kinahan Sandstone.||||||09-NOV-06
13010|Mount Parker Sandstone|22547|5|Briefly described|p21|||In the Texas Downs Basin - mapped as Texas Downs Formation.||||||09-NOV-06
13010|Mount Parker Sandstone|22716|5|Briefly described|table4, p236|Mesoproterozoic|Mesoproterozoic|May be equivalent to part of the Birrindudu Group.||||||
13010|Mount Parker Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|||||||
13010|Mount Parker Sandstone|22764|4|Described|Table1,p7||Carpentarian|770 m. Unconformable on Olympio Formation and Lamboo Complex.||||||01-FEB-10
13010|Mount Parker Sandstone|23314|5|Briefly described|329|||Mount is Mt. in text.||||||
13010|Mount Parker Sandstone|23621|5|Briefly described|p31|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||
13010|Mount Parker Sandstone|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Osmond Basin. Mount is Mt in text. Correlates with Campbell Springs Dolostone (Birrindudu Basin), Shillinglaw Formation (Tennant Creek Inlier) and Barney Creek Formation (McArthur Basin).||||||22-MAY-08
13010|Mount Parker Sandstone|28255|6|Mentioned|p11|||Age is probably Adelaidean or may be as old as Carpentarian. East Kimberley area (WA). Mount is Mt in text.||||||
13010|Mount Parker Sandstone|29805|6|Mentioned|p8|||||||||
13010|Mount Parker Sandstone|29809|6|Mentioned|p418|||||||||
13010|Mount Parker Sandstone|29813|4|Described|Table 2|||||||||
13010|Mount Parker Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13010|Mount Parker Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Carpentarian|Prob. Adelaidean||||||
13010|Mount Parker Sandstone|31393|6|Mentioned|Pl.25|||||||||
13010|Mount Parker Sandstone|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|32660|5|Briefly described|Table 6|||||||||
13010|Mount Parker Sandstone|32728|5|Briefly described|p42|||||||||
13010|Mount Parker Sandstone|34230|6|Mentioned|Plate 8|Proterozoic|Proterozoic|||||||28-OCT-04
13010|Mount Parker Sandstone|35120|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|35950|6|Mentioned|p311|||||||||
13010|Mount Parker Sandstone|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13010|Mount Parker Sandstone|36551|6|Mentioned|p26|||||||||
13010|Mount Parker Sandstone|36885|4|Described|p177|||||||||
13010|Mount Parker Sandstone|36898|6|Mentioned|Fig.2A|||||||||
13010|Mount Parker Sandstone|37299|6|Mentioned|Fig.1|||||||||
13010|Mount Parker Sandstone|37462|4|Described|Table 4.V|||||||||
13010|Mount Parker Sandstone|41811|6|Mentioned|p212|||||||||
13010|Mount Parker Sandstone|43631|6|Mentioned|p20|||||||||
13010|Mount Parker Sandstone|44140|5|Briefly described|p299|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin.||||Correlated with Colombo Sandstone (Kimberley Basin).||
13010|Mount Parker Sandstone|44155|4|Described|p251-252|Mesoproterozoic|Mesoproterozoic|150-300m thick. Type locality at Mount Parker. Probable part correlative of Tawallah and McArthur Groups in McArthur Basin.||||Overlies Red Rock Beds and Fish Hole Dolerite unconformably. Overlain by Bungle Bungle Dolomite conformably. Correlated with Gardiner Sandstone.|Clean quartz sandstone, commonly with pebbly lenses; commonly ferruginous at top.|
13010|Mount Parker Sandstone|44317|4|Described|Table 2||Carpentarian|||||||
13010|Mount Parker Sandstone|44318|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
13010|Mount Parker Sandstone|44324|14|Not recorded|p.10||Neoproterozoic|Tb.2 (Upper Proterozoic).||||||
13010|Mount Parker Sandstone|44325|14|Not recorded|map legend||Neoproterozoic|Up.Proterozoic.||||||
13010|Mount Parker Sandstone|44363|5|Briefly described|p.6,13,14,16,17|||Adelaidean or Carpentarian.||||||
13010|Mount Parker Sandstone|44364|14|Not recorded|map legend|||||||||
13010|Mount Parker Sandstone|45047|2|Defined|p74|early Adelaidean|late Carpentarian|See also pp31,35. Early Adelaidean or Late Carpentarian.||||||09-NOV-06
13010|Mount Parker Sandstone|45112|6|Mentioned|p15|||||||||
13010|Mount Parker Sandstone|45140|2|Defined|p12-13, p25, p39-41, p58, p60, p74|||See also Appx.p31. Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Mount Parker. Mapped as Kearney Beds by Casey and Wells (1964). The type section is in the Osmond Range, in the Dixon Range sheet area. Forms discontinuous strike ridges. 300m thick. In SW of Gordon Downs map area, this unit included rocks now assigned to Wade Creek Sandstone (Gemuts and Smith, 1968).||||Unconformably overlies Olympio Formation. Is overlain conformably by Bungle Bungle Dolomite. Probable equivalent to Birrindudu Group.|Well-sorted, medium-grained quartz arenite; lesser medium- to coarse-grained sublithic arenite and minor pebbly arenite, conglomerate and local siltstone. Cross-bedding common; some bedding planes are crowded with shale pellets.|
13010|Mount Parker Sandstone|46864|5|Briefly described|p40|||||||||
13010|Mount Parker Sandstone|48950|6|Mentioned|p36|||||||||
13010|Mount Parker Sandstone|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Halls Creek Province.||||||07-FEB-11
13010|Mount Parker Sandstone|64104|6|Mentioned|p75, p76 fig 10|Neoproterozoic|Neoproterozoic|Osmond Basin. Part of Osmond Range succession. [this article changes the age of a number of units, including this one, without explanation]||||||19-MAY-15
13010|Mount Parker Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Well sorted thinly bedded medium grained quartz sandstone, medium to coarse sublithic arenite and minor pebble conglomerate with siltstone locally near the base; low angle cross bedding is common, and clay pellets occur on bedding planes in places|
13010|Mount Parker Sandstone|73255|6|Mentioned|p534 Fig.2|Tonian|Tonian|Written as Mt Parker Sandstone in text.||Osmond Range Succession||Underlies the Bungle Bungle Dolomite.||
13017|Mount Percy Lamproite|41158|6|Mentioned|Table 32|||||||||
13030|Mount Pierre Group|38263|6|Mentioned|p16|||||||||
13030|Mount Pierre Group|42994|6|Mentioned|p131|||||||||
13030|Mount Pierre Group|43723|6|Mentioned|p62|||'informal'?||||||
13030|Mount Pierre Group|44403|2|Defined|p.8, Tb.1|Famennian|Frasnian|E/51-12, contains the Virgin Hills Formation and the Gogo Formation. Famennian and Frasnian.||||||
13030|Mount Pierre Group|44404|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
13030|Mount Pierre Group|44998|2|Defined|p.41|||Cont.Gogo & Virgin Hills Formations. Similar to Fossil Downs Formation. Interfingers with Pillara Formation. See also p37-9,43.||||||
13030|Mount Pierre Group|45015|5|Briefly described|p47|Frasnian|Frasnian|Correlated with Gneudna Formation. Geological Province: Fitzroy Basin.||||||01-JUN-06
13030|Mount Pierre Group|48831|14|Not recorded|p.44,45,48-50|||||||||
13030|Mount Pierre Group|48837|14|Not recorded|p.28|||||||||
13030|Mount Pierre Group|48848|14|Not recorded|p.41|||||||||
13036|Mount Pleasant Gabbro|41371|6|Mentioned|Fig.1|||||||||
13036|Mount Pleasant 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, 100k_geologysub10_lut.csv.|2702-2692 Ma (inferred)||||Quartz-bearing gabbro locally grading into granophyre; iron-rich granophyre marker horizon at top; metamorphosed; pyroxene, massive olivine cumulate (dunite) at base; metamorphosed.|
13071|Mount Robinson Ophiolites|30900|6|Mentioned|p67|||On Table 1||||||
13071|Mount Robinson Ophiolites|34324|6|Mentioned|p122|||Table||||||
13071|Mount Robinson Ophiolites|37373|6|Mentioned|Table 2.I|||||||||
13071|Mount Robinson Ophiolites|73391|6|Mentioned|Appendices.|||Glikson (1971). Regional stratigraphic correlation chart of other workers.|||||Basalt, dolerite, pyroxenite.|
13092|Mount Sefton greenstones|31092|6|Mentioned|p4|||||||||
13203|Mount Webb Granite|22716|6|Mentioned|p232|Statherian|Statherian|||||||
13203|Mount Webb Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
13203|Mount Webb Granite|23396|6|Mentioned|p426|||||||||
13203|Mount Webb Granite|24197|5|Briefly described|p33, p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of Mount Webb Suite. Heterogeneous granite, of several types of unaltered granite, sodic-clacic altered granite, sericite-altered granite and aplite. Age: 1615Ma. Geol. Prov: western Arunta Block. See also p143, p146 for lith.detail.||||||30-JAN-17
13203|Mount Webb Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1480Ma. Geological Province: Arunta Inlier. Name written as Mt Webb only under heading for GRANITE.||||||09-MAY-05
13203|Mount Webb Granite|29806|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|29807|4|Described|Table 1|||||||||
13203|Mount Webb Granite|35201|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|35223|4|Described|Table.2|||||||||
13203|Mount Webb Granite|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13203|Mount Webb Granite|39559|6|Mentioned|Table 1|||||||||
13203|Mount Webb Granite|39888|6|Mentioned|Fig.9|||||||||
13203|Mount Webb Granite|41465|6|Mentioned|p13|||||||||
13203|Mount Webb Granite|42504|5|Briefly described|p61|||||||||
13203|Mount Webb Granite|44194|4|Described|p2|Paleoproterozoic|Paleoproterozoic|Co-magmatic with Pollock Hills Formation Felsic Volcanics. SHRIMP ages given 1639+/-5 Ma.||||||07-NOV-08
13203|Mount Webb Granite|45140|2|Defined|p12-13, p22, p26, p28-38, p60-61, p74|Calymmian|Calymmian|See also Appx.p14-15. Blake (1977). Arunta Block. Named after a prominent hill (Mount Webb). Forms scattered groups of spherical boulders and tors up to 30m high; one of these is the type locality, at 22deg 50'00"S, 127deg 50'30"E. A preferred age given is 1526 +/- 25 Ma (Page et al., 1976). Geochemistry detailed.|1520 +/- 40 Ma (Rb-Sr; Page et al., 1976).|||Intrudes Arunta Complex, also (and probably co-magmatic with lavas in) the Pollock Hills Formation. Is overlain unconformably by Heavitree Quartzite.|Pink to grey, medium- to coarse-grained biotite adamellite, locally with hornblende. Locally has a gneissic texture. Cut by rare aplite veins <1m wide, by quartz veins, and by later unfoliated basic dykes.|
13203|Mount Webb Granite|46788|4|Described|p7|||||||||
13203|Mount Webb Granite|50369|5|Briefly described|p1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Mount Web Suite. Age: 1486 +/- 40Ma.||||||07-NOV-08
13203|Mount Webb Granite|61660|5|Briefly described|p23. |Proterozoic|Proterozoic|Western extension of the Warumpi Province.|1639 +/- 5 Ma.|||||
13203|Mount Webb Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Monzogranite; syenogranite, granodiorite, and tonalite.||||||09-DEC-08
13203|Mount Webb Granite|64726|6|Mentioned|p84.|Paleoproterozoic|Paleoproterozoic|||||||
13203|Mount Webb Granite|65074|4|Described|p351, p354 Tb. 4-11, p360-362|Mesoproterozoic|Mesoproterozoic|Type section 32 km WNW of Mount Webb. Probably comagmatic with acid lavas of Pollock Hills Formation.|1520 +/- 40 Ma (Page et al., 1976).|||Intrudes Pollock Hills Formation. Overlain by Heavitree Quartzite unconformably.|Even-grained adamellite.|
13203|Mount Webb Granite|67323|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|~1640 Ma.||||Heterogeneous granite, hornblende-biotite granite, sodic-calcic altered granite, sericite-altered granite, aplite.|
13203|Mount Webb Granite|68994|4|Described|p1, p4-9, p11, p17-18, p23, p26-27|||Warumpi Province. Magmatic crystallisation age. Similar age determinations given. Hf analyses detailed.|1640+/-7 Ma (Kirkland et al. 2009).||||Felsic magmatic rocks. Sample analysed is coarse-grained, foliated, biotite-hornblende metamonzogranite.|13-JAN-17
13203|Mount Webb Granite|69003|5|Briefly described|p5, p32|Paleoproterozoic|Paleoproterozoic|Warumpi Province, West Arunta Orogen. Associated with the c.1640-1635 Ma Liebig Orogeny.|c.1640 Ma.|||Intrudes Ininti Granite.||
13203|Mount Webb Granite|69031|5|Briefly described|p4, p6, p7-8, p12, p15, p27,p43,p59,p67|Statherian|Statherian|Warumpi Province, Arunta Orogen. Previously thought to be coeval with Pollock Hills Formation; geochronology establishes a c.30 m.y. separation. Several similar age determinations given. A large gold (and numerous other metals) anomaly occurs in regolith within this unit's area. Magnetic susceptibility data. Distance to this unit was used as a predictor in modelling for U sources and orogenic Au systems.|1640 +/- 7 Ma (Kirkland et al., 2009).||||Granite, granodiorite, aplite, albitite, porphyry, tonalite. Has undergone local extensive magmatic sodic-calcic and sericitic alteration.|
13203|Mount Webb Granite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Metamonzogranite, metasyenogranite, metagranodiorite and metatonalite.|
13203|Mount Webb Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
13203|Mount Webb Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
13203|Mount Webb Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1640+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
13203|Mount Webb Granite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1640 Ma.||||Metamonzogranite; locally metasyenogranite, metagranodiorite, and metatonalite.|
13203|Mount Webb Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|Max age 1647+/-7 Ma, min 1633+/-7 Ma.||||Metamonzogranite; metasyenogranite, metagranodiorite, and metatonalite.|
13210|Mount West Gabbro|30390|4|Described|p146|||||||||
13280|Mowbowra Conglomerate Member|23726|5|Briefly described|p91|||Of Bundera Calcarenite. Geological Province: Carnarvon Basin.||||||
13280|Mowbowra Conglomerate Member|37016|6|Mentioned|Map legend|Holocene|Pleistocene|Pleistocene to Holocene.||||||
13280|Mowbowra Conglomerate Member|39427|4|Described|Table 1|||See also P16||||||
13280|Mowbowra Conglomerate Member|41271|4|Described|p195|||||||||
13280|Mowbowra Conglomerate Member|42116|5|Briefly described|p71|||||||||
13285|Mowla Sandstone|7433|4|Described|p25 Fig.2, p42, p44. |Cretaceous|Jurassic|See also Mowla Formation (p45 Fig.35). Canning Basin. Thickness up to 15 m. Plant-bearing sandstones. Isolated hilltop exposures in Edgar Ranges area.||||Conformably and disconformably overlies Jarlemai Siltstone.|Fluvial to deltaic sandstone; discontinuous basal conglomerate and mudstone.|
13285|Mowla Sandstone|22767|5|Briefly described|Table3 P12, P23|Early Cretaceous|Late Jurassic|Probably equivalent to the Broome Sandstone||||||
13285|Mowla Sandstone|23212|4|Described|Table.1 p11|Early Cretaceous|Late Jurassic|||||||
13285|Mowla Sandstone|32648|6|Mentioned|p32|||L. Cret.||||||
13285|Mowla Sandstone|36257|6|Mentioned|Table 2.1|||||||||
13285|Mowla Sandstone|36634|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13285|Mowla Sandstone|36890|3|Fully described|p352|||Formerly Mowla Conglomerate.||||||09-DEC-08
13285|Mowla Sandstone|37369|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13285|Mowla Sandstone|38878|6|Mentioned|Map legend|Neocomian|Tithonian|Tithonian - Neocomian||||||
13285|Mowla Sandstone|44143|4|Described|p.432 Table 4-19; p.442, Figure 4-96|Cretaceous|Jurassic|Up to 15m thick; fine to very coarse sandstone; granule and clay pellet conglomerate; fluvial to deltaic. Conformably overlies Jarlemai Siltstone. Type section near Mowla Bluff (MOUNT ANDERSON: 18deg 49' 20" S, 123deg 43' 50" E). Contains plant fossils.||||||23-NOV-17
13285|Mowla Sandstone|44998|2|Defined|p182|Neocomian|Tithonian|u.Tithonian-l.Neocomian. On many pages. p.133,147,185,188, map.||||||
13285|Mowla Sandstone|45153|2|Defined|App.6-124|Late Jurassic|Late Jurassic|Formerly Mowla Conglomerate.||||||09-DEC-08
13285|Mowla Sandstone|45158|3|Fully described|p14|||||||||
13285|Mowla Sandstone|48826|14|Not recorded|Tb.III|||Correlates with Godfrey Beds.||||||
13285|Mowla Sandstone|64580|4|Described|map legend||Early Cretaceous|Fine- to coarse-grained sandstone; minor mudstone and conglomerate.||||||09-DEC-08
13285|Mowla Sandstone|69297|6|Mentioned|p337, p352|Valanginian|Valanginian|Broome Platform of the Canning Basin.||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Broome Sandstone.||
13285|Mowla Sandstone|69590|4|Described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
13285|Mowla Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
13285|Mowla Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Lower Cretaceous|Lower Cretaceous||100-145 Ma||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
13285|Mowla Sandstone|71267|5|Briefly described|1m_geologyp12_lithology_lut.csv|Early Cretaceous|Early Cretaceous|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 500k_interpgeop16_lut.csv.|145-113 Ma (biostrat)||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
13285|Mowla Sandstone|72034|6|Mentioned|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Shown informally grouped with Broome and Melligo Sandstones. Siliciclastic Canning Basin unit.  Age from biostratigraphy.||||||
13286|Moyagee Formation|29690|4|Described|p10|||||||||
13286|Moyagee Formation|30491|4|Described|p9|||Archaean||||||
13286|Moyagee Formation|30882|6|Mentioned|p47|||Refers de la Hunty (in press).||||||
13286|Moyagee Formation|30949|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
13286|Moyagee Formation|30960|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
13286|Moyagee Formation|35269|6|Mentioned|p298|||||||||
13286|Moyagee Formation|36870|3|Fully described|p56|||||||||
13286|Moyagee Formation|38492|5|Briefly described|Table 2|||||||||
13286|Moyagee Formation|41066|6|Mentioned|1 of 2 N03|||||||||
13286|Moyagee Formation|41841|5|Briefly described|Table 1|||Article recommends adandoning this name use. See p55||||||
13287|Moyle River Formation|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||Of the Fitzmaurice Group.||||
13287|Moyle River Formation|22547|6|Mentioned|Fig4,p25|||Of the Fitzmaurice Group. Overlain by Goobaieri Formation.||||||14-NOV-06
13287|Moyle River Formation|23822|5|Briefly described|p299|Proterozoic|Proterozoic|Geological Province: Litchfield Province.||||||
13287|Moyle River Formation|32171|4|Described|Table 1|||Carpentarian/Adelaidean||||||
13287|Moyle River Formation|32307|4|Described|Table 2|||Proterozoic||||||
13287|Moyle River Formation|32309|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian/Adelaidean||||||
13287|Moyle River Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
13287|Moyle River Formation|32660|5|Briefly described|Table 6|||||||||
13287|Moyle River Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone; minor siltstone, grit and pebble conglomerate.||||||02-DEC-04
13287|Moyle River Formation|32701|4|Described|Table 1|||Adelaidean. Fitzmaurice Group.||||||13-NOV-06
13287|Moyle River Formation|32728|6|Mentioned|Fig.14|||||||||
13287|Moyle River Formation|33076|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|33093|4|Described|Table 2|||||||||
13287|Moyle River Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|35140|6|Mentioned|p322|||||||||
13287|Moyle River Formation|37462|6|Mentioned|Fig.4.13|||||||||
13287|Moyle River Formation|39889|6|Mentioned|p485|||||||||
13287|Moyle River Formation|40495|6|Mentioned|p12|||||||||
13287|Moyle River Formation|40764|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13287|Moyle River Formation|40765|3|Fully described|p10|||||||||
13287|Moyle River Formation|41645|4|Described|p135|||||||||
13287|Moyle River Formation|41646|6|Mentioned|Map legend|Mesoproterozoic||Of the Fitzmaurice Group. Quartzarenite, fine to medium grained, poorly sorted, thickly bedded to massive, with abundant cross bedding; basal conglomerate; stromatolitic dolomite; dolomite; siltstone.||||||17-OCT-05
13287|Moyle River Formation|41661|6|Mentioned|p16|||||||||
13287|Moyle River Formation|45112|6|Mentioned|Table 16|||||||||
13287|Moyle River Formation|47047|6|Mentioned|p220|||||||||
13287|Moyle River Formation|48938|2|Defined|p15|Adelaidean|Adelaidean|||||||
13287|Moyle River Formation|48942|3|Fully described|p32|||Strat. section p108.||||||13-NOV-06
13287|Moyle River Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Silica-cemented quartz sandstone, minor siltstone and pebble conglomerate.||||||07-JAN-09
13287|Moyle River Formation|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: ~100m. Unconformably overlies Bow River Granite. Conformably overlain by Goobaieri Formation. Geological Province: Halls Creek Orogen. Quartz sandstone, minor siltstone and conglomerate.||||||
13287|Moyle River Formation|63866|4|Described|p108|Statherian|Statherian|Litchfield Province, Pine Creek Orogen.|c. 1635 Ma (Carson, C.J., unpublished)|Fitzmaurice Group||Intruded by the Murrenja Dolerite.||
13287|Moyle River Formation|64677|5|Briefly described|p13|||Pine Creek Orogen.||Fitzmaurice Group.||Nonconformably overlies Koolendong Granite.||
13287|Moyle River Formation|64698|4|Described|lithinterp table|||Age ~1150-1250Ma (Stenian) but age name given as Statherian. Victoria - Birrindudu Basin. Of Fitzmaurice Group. Max. thickness 3000m. Silica cemented quartz sandstone, minor siltstone and pebble conglomerate.||||||07-JAN-09
13287|Moyle River Formation|64956|6|Mentioned|p66|||Overlies the Wagait Granite.||||||07-FEB-11
13287|Moyle River Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Silica cemented quartz sandstone, minor siltstone and pebble conglomerate||||||
13287|Moyle River Formation|65417|5|Briefly described|p158 Fig.2.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone.||Basal unit in Fitzmaurice Group.||Is overlain conformably by Goobaieri Formation.||
13287|Moyle River Formation|67167|5|Briefly described|Map legend.|||||Unit in Fitzmaurice Group.|||Quartz sandstone, fine- to medium-grained, poorly sorted, thickly bedded to massive, with abundant cross-beds, basal conglomerate; dolostone, siltstone.|
13287|Moyle River Formation|67186|5|Briefly described|Map legend.|||||Unit in Fitzmaurice Group.|||Quartz sandstone, fine- to medium-grained, poorly-sorted, thickly-bedded to massive, with abundant cross-beds; basal conglomerate; dolostone; siltstone.|23-NOV-11
13287|Moyle River Formation|69420|6|Mentioned|p5:105||||||||Arenite and intraformational conglomerate.|12-JUL-16
13287|Moyle River Formation|69435|4|Described|p20:2-5|||Sweet et al. (1974). Fitzmaurice Basin. Thickness estimated at about 5,000m; it is not possible to determine the true thickness of this unit: previous estimates are briefly discussed. Has developed a weak to moderate foliation adjacent to faults in the north. Is intruded by Murrenja Dolerite.|<1640 Ma (detrital zircons).|Fitzmaurice Group.||Unconformably overlies Bow River and Koolendong Granites, Murra-Kamangee Granodiorite, Hermit Creek Metamorphics and Henschke Breccia. Is overlain conformably by Goobaieri Formation.|Fine- to coarse-grained quartz sandstone; minor siltstone and pebble to cobble conglomerate. Local;ly contains small lenses of volcanic rocks, dolostone (with stromatolites) and conglomerate.|12-JUL-16
13287|Moyle River Formation|69673|5|Briefly described|p59, p60 fig 48|Statherian|Statherian|Up to 5000m thick.|1640 Ma|Fitzmaurice Group||Overlain by Goobaieri Formation|Fine to coarse grained quartz sandstone, minor siltstone and conglomerate.|
13287|Moyle River Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Silica cemented quartz sandstone, minor siltstone and pebble conglomerate.|
13287|Moyle River Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
13287|Moyle River Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1638+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
13298|Muchea Limestone|23816|6|Mentioned|p257|||Geological Province: Perth Basin.||||||16-DEC-04
13298|Muchea Limestone|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
13298|Muchea Limestone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||24-NOV-09
13298|Muchea Limestone|30939|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
13298|Muchea Limestone|33044|4|Described|p57|||See also map 3.||||||
13298|Muchea Limestone|35638|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
13298|Muchea Limestone|36293|6|Mentioned|p217|||||||||
13298|Muchea Limestone|36890|4|Described|p257|||||||||
13298|Muchea Limestone|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
13298|Muchea Limestone|39554|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
13298|Muchea Limestone|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
13298|Muchea Limestone|41344|6|Mentioned|p123|||||||||
13298|Muchea Limestone|41346|6|Mentioned|p72|||||||||
13298|Muchea Limestone|41783|4|Described|p48|||||||||
13298|Muchea Limestone|44144|4|Described|p501 Tb.4-21|Quaternary|Quaternary|No type section.  1m thick lacustrine deposits; some kankar development.||||Overlies Guildford Formation.|Marly limestone; in places algal laminated.|
13298|Muchea Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||lacustrine sediment|
13315|Muderong Shale|6876|6|Mentioned|p100 Fig.5, pp102-105|Early Cretaceous|Early Cretaceous|Post-dates the deltas which largely comprise the Barrow Group.||||||
13315|Muderong Shale|12471|5|Briefly described|p475, Fig 2.|Early Cretaceous|Early Cretaceous|Forms a seal over the Breakup Unconformity in Peedamullah Shelf; contains over 50 m of shale. See also Figs 3, 4.||Unit in Winning Group.|Includes Windalia Sandstone Member and Mardie Greensand Member.|Overlies Mungaroo Formation. Is overlain by Windalia Radiolarite.||27-OCT-14
13315|Muderong Shale|12491|5|Briefly described|p448, pp458-462.|Late Cretaceous|Early Cretaceous|Forms a regional seal over Early Cretaceous and older sediments in the Carnarvon Basin. See also Muderong Formation in this paper.|||Includes Mardie Greensand Member.|Overlies Zeepaard and Birdrong Formations and Barrow Group. Is overlain by Windalia Radiolarite and Gearle Formation.||06-NOV-14
13315|Muderong Shale|12498|6|Mentioned|p517 Fig.3. |Early Cretaceous|Early Cretaceous|||||||
13315|Muderong Shale|12729|6|Mentioned|p. 15, 32||Cretaceous|Low-energy, offshore-marine shale.||Winning Group|Windalia Sandstone Member|Underlain by the Birdrong Sandstone, overlain by the Windalia Radiolarite.||
13315|Muderong Shale|12731|6|Mentioned|p596.|||Acted as a seal for the shallow Birdrong Sandstone reservoir in northern Gascoyne Platform.||||||
13315|Muderong Shale|13353|6|Mentioned|p412.|||Dampier Sub-basin. Well-documented hydrocarbon source potential.||||||
13315|Muderong Shale|13615|3|Fully described|p1, p4-5, p6-8, p14, p18-20,|Aptian|Valanginian|Peedamullah Shelf. Commonly <200m thick onshore and reaches a maximum >300m thick offshore.b Spores/Pollen Zone and Dinoflagellate zones provided. Seals the Tubridgi gasfield. Intersected in numerous drillholes. This unit together with the Windalia Radiolarite are the best potentital cretaceous source rocks in the Peedamullah Shelf. Type section is in Northwest Kennedy Range; 24deg08'10"S 114deg45'50"E. Contains abundant microfossils. Deposited in a low energy marine shelf environment. See also p24, p29-31, p34-36, p38-p43, p46-49, p51, p53-54, p56, p58-p60, p62-73, p81-83, p85-88, p101, 102 App. 3, Plates 2,3.||Of Winning Group.|Includes the Windalia Sandstone Member.|Overlies the Mardie Greensand and conformably overlies the Birdrong Sandstone. Unconformably overlies the Mungaroo Formation. Overlain by the Windalia Radiolarite.|Clayey grey siltstone, lesser shale, fine sandstone and greensand.|12-FEB-19
13315|Muderong Shale|14228|5|Briefly described|p5 fig 2, p9, p18-19, p26 |Aptian|Barremian|A proven seal in Northern Carnarvon Basin. Seals Birdrong Sandstone.||Winning Group||Overlies Birdrong Sandstone. Overlain by Windalia Radiolarite.|Medium- to dark-grey shale.|
13315|Muderong Shale|22703|4|Described|p115,118-9,126 Fig.3|Aptian|Valanginian|||||||
13315|Muderong Shale|23311|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group.||||||
13315|Muderong Shale|23312|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Winning Group.||||||
13315|Muderong Shale|23355|5|Briefly described|8 Fig.1|Early Cretaceous|Early Cretaceous|||||||
13315|Muderong Shale|23359|5|Briefly described|79|||||||||
13315|Muderong Shale|23379|4|Described|p160 Fig.2, p158-162,164,165,168,171-173|Aptian|Valanginian|of Barrow Sub-basin.||||||
13315|Muderong Shale|23403|4|Described|p9|Late Cretaceous|Early Cretaceous|Of Winning Group.||||||24-NOV-09
13315|Muderong Shale|23433|5|Briefly described|p111|Early Cretaceous|Early Cretaceous|||||||
13315|Muderong Shale|23535|4|Described|p125 Fig 3|||Large fossil assemblage. Of Condon (1957, 1968). Underlying unit Birdrong Sandstone (u).||||||
13315|Muderong Shale|23572|4|Described|p11|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Of the Winning Group. Underlying Unit: Birdrong Sandstone. Overlying Unit: Windalia Radiolarite.||||||12-MAY-05
13315|Muderong Shale|23726|6|Mentioned|p8 Fig 2c|||Underlying unit Birdrong Sandstone.  Geological Province: Carnarvon Basin.||||||
13315|Muderong Shale|23815|4|Described|p296|Aptian|Aptian|Geological Province: Carnarvon Basin. Underlying unit: Birdrong Sandstone (conformable). Overlying unit: Windalia Radiolarite (conformable). Max. thickness: 266 m.||||||
13315|Muderong Shale|23915|5|Briefly described|p518 Table 1|Cretaceous|Cretaceous|Geologicalprovince: Southern Carnarvon Basin.||||||
13315|Muderong Shale|23935|4|Described|p11 Fig.7, p12 Fig.8|Aptian|Barremian|Of Winning Group. Conformably overlies Birdrong Sandstone. Disconformably overlain by Windalia Radiolarite. Light to medium grey siltstone and soft pyritic mudstone. Thickness: 14 m. Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
13315|Muderong Shale|24059|5|Briefly described|p132|Late Cretaceous|Early Cretaceous|Of Winning Group. Geological Province: Barrow Sub-basin.||||||
13315|Muderong Shale|24084|5|Briefly described|p146 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
13315|Muderong Shale|24160|5|Briefly described|p36, 39|Cretaceous|Cretaceous|Carnarvon Basin. Hosts bentonite deposits.||Winning Group||Overlies Birdrong Sandstone. Is overlain conformably by Windalia Radiolarite.|Clayey siltstone and fine-grained sandstone.|
13315|Muderong Shale|24205|4|Described|p241-242|Aptian|Neocomian|Claystone, siltstone with dominant smectite.  Overlies the Mardie Greensand and Birdrong Sandstone conformably.  Geological Province: Northern Carnarvon Basin.||||||
13315|Muderong Shale|24246|5|Briefly described|p18, 19|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin.||||||
13315|Muderong Shale|24315|6|Mentioned|p43|||Geological Province: Barrow Sub-Basin.||||||
13315|Muderong Shale|24331|5|Briefly described|p475|||Conformably overlies Maride Greensand, which grades up into it. Conformably overlain by Windalia Sand Member. Geological Province: Barrow Sub-basin.||||||22-FEB-05
13315|Muderong Shale|24351|5|Briefly described|Plate 4 (in pocket)|Early Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province :Exmouth Plateau, Exmouth Sub-basin, Gascoyne Platform/Sub-basin.||||||13-DEC-07
13315|Muderong Shale|24409|5|Briefly described|p48|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin||||||
13315|Muderong Shale|24410|5|Briefly described|p213|||Conformably overlain by Windalia Radiolarite (Winning Group). Geological Province: Carnarvon Basin.||||||24-NOV-09
13315|Muderong Shale|24541|6|Mentioned|p64|Early Cretaceous|Early Cretaceous|||||||
13315|Muderong Shale|29381|4|Described|p67|||||||||
13315|Muderong Shale|29721|6|Mentioned|Table 102|||||||||
13315|Muderong Shale|30016|6|Mentioned|p92|||||||||
13315|Muderong Shale|30110|6|Mentioned|p81|||part of Winning Group.||||||
13315|Muderong Shale|30264|6|Mentioned|p30|||Lower Cretaceous age||||||
13315|Muderong Shale|30304|4|Described|p52|||Aptian.Nomencl.not accord with Code.Incls.Windalia Sd,Muderong Grnsd Mbr||||||
13315|Muderong Shale|30365|6|Mentioned|Fig.8|||||||||
13315|Muderong Shale|31083|6|Mentioned|p455|||||||||
13315|Muderong Shale|31561|4|Described|p38|||See also P34. Early Cretaceous||||||
13315|Muderong Shale|31604|6|Mentioned|p6|||See also Table 4. Aptian||||||
13315|Muderong Shale|32166|4|Described|p159|||||||||
13315|Muderong Shale|32641|6|Mentioned|p6|||Cretaceous.||||||
13315|Muderong Shale|32642|6|Mentioned|p76|||||||||
13315|Muderong Shale|32648|6|Mentioned|p32|||Winning Gp.||||||
13315|Muderong Shale|32711|6|Mentioned|Fig.3|||||||||
13315|Muderong Shale|32714|6|Mentioned|Fig.7|||L.Cret. Winning Gp.||||||
13315|Muderong Shale|32715|6|Mentioned|Fig.16|||||||||
13315|Muderong Shale|33100|6|Mentioned|p191|||||||||
13315|Muderong Shale|33165|6|Mentioned|Chart|||Correlation chart only||||||
13315|Muderong Shale|33386|6|Mentioned|Fig.7|||||||||
13315|Muderong Shale|33450|6|Mentioned|Fig.5|||See P11.||||||
13315|Muderong Shale|33453|4|Described|p72|||||||||
13315|Muderong Shale|34363|6|Mentioned|p56|||See also P57, Figs.7 & 8. Aptian.||||||
13315|Muderong Shale|34838|6|Mentioned|p3|||||||||
13315|Muderong Shale|34840|6|Mentioned|p68|||||||||
13315|Muderong Shale|34846|6|Mentioned|Fig.3|||||||||
13315|Muderong Shale|35105|6|Mentioned|Fig.5|||||||||
13315|Muderong Shale|35144|6|Mentioned|p4|||||||||
13315|Muderong Shale|35282|6|Mentioned|Fig.19|||||||||
13315|Muderong Shale|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
13315|Muderong Shale|35983|6|Mentioned|p147|||See also Table 27.||||||
13315|Muderong Shale|36093|6|Mentioned|Fig.2|||||||||
13315|Muderong Shale|36257|6|Mentioned|Table 2.1|||||||||
13315|Muderong Shale|36266|6|Mentioned|p152|||||||||
13315|Muderong Shale|36613|6|Mentioned|p1865|||||||||
13315|Muderong Shale|36751|6|Mentioned|p488|||||||||
13315|Muderong Shale|36890|3|Fully described|p296|||||||||
13315|Muderong Shale|36902|6|Mentioned|p22|||||||||
13315|Muderong Shale|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
13315|Muderong Shale|37306|6|Mentioned|p43|||||||||
13315|Muderong Shale|37320|6|Mentioned|p235|||||||||
13315|Muderong Shale|37360|6|Mentioned|p573|||||||||
13315|Muderong Shale|37422|6|Mentioned|p6|||||||||
13315|Muderong Shale|37577|6|Mentioned|p8|||See also P76.||||||
13315|Muderong Shale|37689|6|Mentioned|p24|||||||||
13315|Muderong Shale|38482|6|Mentioned|p22|||||||||
13315|Muderong Shale|38484|6|Mentioned|p9|||||||||
13315|Muderong Shale|38485|4|Described|p15|||||||||
13315|Muderong Shale|38655|6|Mentioned|p8|||||||||
13315|Muderong Shale|39158|5|Briefly described|p36|||||||||
13315|Muderong Shale|39211|6|Mentioned|p58|||Late Neocomian||||||
13315|Muderong Shale|39427|4|Described|Table 1|||||||||
13315|Muderong Shale|39486|6|Mentioned|p2092|||||||||
13315|Muderong Shale|39757|6|Mentioned|p1605|||||||||
13315|Muderong Shale|40170|6|Mentioned|p156|||||||||
13315|Muderong Shale|40306|6|Mentioned|p58|||||||||
13315|Muderong Shale|40342|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
13315|Muderong Shale|40343|5|Briefly described|p11|||||||||
13315|Muderong Shale|40395|6|Mentioned|p316|||||||||
13315|Muderong Shale|40617|6|Mentioned|p12|||||||||
13315|Muderong Shale|40800|6|Mentioned|Fig.2|||||||||
13315|Muderong Shale|40801|6|Mentioned|p42|||||||||
13315|Muderong Shale|40992|6|Mentioned|p13|||||||||
13315|Muderong Shale|41125|5|Briefly described|p41|||||||||
13315|Muderong Shale|41170|6|Mentioned|p152|||||||||
13315|Muderong Shale|41271|3|Fully described|p148|||||||||
13315|Muderong Shale|41436|6|Mentioned|p48|||||||||
13315|Muderong Shale|41438|6|Mentioned|p108|||||||||
13315|Muderong Shale|41439|5|Briefly described|p122|||||||||
13315|Muderong Shale|41440|4|Described|p138|||||||||
13315|Muderong Shale|41441|6|Mentioned|p153|||||||||
13315|Muderong Shale|41443|4|Described|p164|||||||||
13315|Muderong Shale|41444|6|Mentioned|Fig.4|||||||||
13315|Muderong Shale|41445|6|Mentioned|p197|||||||||
13315|Muderong Shale|41446|6|Mentioned|p203|||||||||
13315|Muderong Shale|41447|6|Mentioned|p226|||See also P234||||||
13315|Muderong Shale|41589|6|Mentioned|p118|||||||||
13315|Muderong Shale|41709|6|Mentioned|p213|||||||||
13315|Muderong Shale|41712|6|Mentioned|Fig.8|||||||||
13315|Muderong Shale|41732|5|Briefly described|p540|||||||||
13315|Muderong Shale|42150|6|Mentioned|p65|||||||||
13315|Muderong Shale|42395|6|Mentioned|Fig.22 P85|||||||||
13315|Muderong Shale|42463|6|Mentioned|Fig.2 P169|||||||||
13315|Muderong Shale|42598|4|Described|p97, p40|Aptian|Valanginian|Age: middle Neocomian (Valanginian) to Aptian||||||
13315|Muderong Shale|42615|6|Mentioned|p6|||Triassic||||||
13315|Muderong Shale|43173|6|Mentioned|16|Neocomian|Tithonian|||||||
13315|Muderong Shale|43564|6|Mentioned|p445|||||||||
13315|Muderong Shale|43712|5|Briefly described|p11|||||||||
13315|Muderong Shale|43722|5|Briefly described|p10-11|||||||||
13315|Muderong Shale|43724|5|Briefly described|p29|||||||||
13315|Muderong Shale|43824|6|Mentioned|p131|||||||||
13315|Muderong Shale|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
13315|Muderong Shale|43827|5|Briefly described|p193|Aptian|Hauterivian|Found at ODP sites 762,763||||||
13315|Muderong Shale|44159|5|Briefly described|Table p.37||Early Cretaceous|||||||
13315|Muderong Shale|44344|14|Not recorded|p.17,24,opp.4, map||Aptian|Fm of Winning Group; Aptian (or Albian-Cenomanian??). (G50-1).||||||
13315|Muderong Shale|44345|14|Not recorded|map legend||Early Carboniferous|Lower Carboniferous.||||||
13315|Muderong Shale|44537|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
13315|Muderong Shale|44611|14|Not recorded|p20|||||||||
13315|Muderong Shale|44657|14|Not recorded|p.5,6,11|||||||||
13315|Muderong Shale|44937|5|Briefly described|p92||Early Cretaceous|||||||
13315|Muderong Shale|44938|5|Briefly described|p149,152-155||Cretaceous|||||||
13315|Muderong Shale|45004|2|Defined|p.8,17,18,21,24-43|||On many pages. (G50-1/Norton).||||||
13315|Muderong Shale|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||01-JUN-06
13315|Muderong Shale|45104|6|Mentioned|p35|||||||||
13315|Muderong Shale|45142|6|Mentioned|Fig.4|||||||||
13315|Muderong Shale|47053|6|Mentioned|p456|||||||||
13315|Muderong Shale|48610|14|Not recorded|Pl.1,5,6|||||||||
13315|Muderong Shale|48628|14|Not recorded|p.4,5,15,16,23,24|||||||||
13315|Muderong Shale|48858|14|Not recorded|p.5|||||||||
13315|Muderong Shale|48861|2|Defined|p.7|||p.1,5,9. Pl.1.||||||
13315|Muderong Shale|48925|6|Mentioned|p108|||Lower Cretaceous age. Fauna||||||
13315|Muderong Shale|49942|4|Described|p4 Fig.3|Early Cretaceous|Early Cretaceous|Conformably overlain by Windalia Radiolarite. Conformably overlies Birdrong Sandstone. Of Winning Group. Geological Province: Gascoyne Platform.||||||29-APR-13
13315|Muderong Shale|50023|6|Mentioned|p14 (fig.)|||Name appears as Top Muderong Shale in figure.  Geological Province: Carnarvon Basin.||||||
13315|Muderong Shale|50085|5|Briefly described|p23 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
13315|Muderong Shale|60118|5|Briefly described|p29|Early Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province: Northern Carnarvon Basin.||||||
13315|Muderong Shale|60119|6|Mentioned|p26|||Geological Province: Carnarvon Basin.||||||22-JUL-04
13315|Muderong Shale|60379|6|Mentioned|p126 fig 3, p127, 132|Aptian|Barremian|Dampier sub-basin, Carnarvon Basin. Open marine claystone.||||In part equivalent to Saffron Sandstone?||
13315|Muderong Shale|60384|6|Mentioned|p243 Fig 2a, p261|Early Cretaceous|Early Cretaceous|Perth and Carnarvon Basins.||Of Winning Group.||||
13315|Muderong Shale|60386|6|Mentioned|p302|Barremian|Barremian|Perth Basin, Carnarvon Basin. Distal shelf/basin.||||||
13315|Muderong Shale|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|||||||
13315|Muderong Shale|61023|5|Briefly described|p27 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||11-APR-08
13315|Muderong Shale|61554|6|Mentioned|p625 Fig.2|||Barrow Island.||||Overlies Barrow Group.||
13315|Muderong Shale|61811|5|Briefly described|p8, p11, p17.|Cretaceous|Cretaceous|||Unit in Winning Group.|Includes Winning Sandstone Member.|Overlies Birdrong Sandstone. Is overlain by Windalia Radiolarite.||
13315|Muderong Shale|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||
13315|Muderong Shale|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
13315|Muderong Shale|62837|5|Briefly described|Stratigraphic columns|Neocomian|Neocomian|Age: ~135Ma. Geological Province: Exmouth Sub-basin, Barrow Sub-basin and Roebuck Basin; also offshore Canning.||||||01-MAR-10
13315|Muderong Shale|63068|5|Briefly described|p46|||Overlain by Gearle Siltstone,  or by Alinga Formation (southern part of basin). Geological Province: Carnarvon Basin.||||||
13315|Muderong Shale|63950|5|Briefly described|p336 Fig. 4|Aptian|Hauterivian|Overlies Mardie Greensand. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
13315|Muderong Shale|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
13315|Muderong Shale|64635|5|Briefly described|p7 |||||||Includes the Winning Sandstone Member.||
13315|Muderong Shale|64973|4|Described|p504, p504 Fig. 2, p505, p505 Fig. 3|Aptian|Barremian|Of Winning Group. Geological Province: Carnarvon Basin. Consists of a number of progradational cycles and consists of fine-grained sediments. Also on p506 Fig. 4, 506 Fig. 6, p508.||||||
13315|Muderong Shale|64977|5|Briefly described|p491.|Early Cretaceous|Early Cretaceous||||Includes Mardie Greensand Member, Windalia Sand Member and Windalia Radiolarite.|Unconformably overlies Barrow Group and Flacourt Formation. Is overlain by Gearle Siltstone.||
13315|Muderong Shale|64978|6|Mentioned|p528 Fig.2.|Early Cretaceous|Early Cretaceous|||||||
13315|Muderong Shale|65708|6|Mentioned|p107|Aptian|Barremian|North West Shelf. The regional seal, deposited during a Basin-wide marine transgression.||||||29-JUN-22
13315|Muderong Shale|66126|6|Mentioned|p206, 212-213, 215|Early Cretaceous|Early Cretaceous|Carnarvon Basin. Overlies the oil-bearing marine strata of the Stag (oil) Field.|||Tunney Member.|Overlies Mardie Greensand.||
13315|Muderong Shale|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Mudstone.|
13315|Muderong Shale|67200|5|Briefly described|p8 fig 6, p17 table 1|Cretaceous|Cretaceous|Thermal conductivty of 1.69 W/mK. See also  p46, p50, p53, app 2 p5.||Winning Group|Includes Windalia Sandstone Member|Overlies Birdrong Sandstone, Mardie Greenstone, Nanutarra Formation, Yarraloola Conglomerate, overlain by Windalia Radiolarite|Siltstone/Shale and mudstone.|
13315|Muderong Shale|67368|5|Briefly described|p207, p210 Fig.5. |Early Cretaceous|Early Cretaceous|Slow seismic velocity; creates a series of inter-bed multiple generators with the overlying high velocity/amplitude carbonates; this poor quality data had hampered exploration. Improved processing techniques since 2004 have provided significant imaging enhancements; these are detailed in this study. Regional seal.||||Overlies Forestier Claystone. Is overlain by Windalia Radiolarite.||
13315|Muderong Shale|67784|5|Briefly described|p26, p30-34|Aptian|Barremian|Age derived from Sr Isotopic data.|||Includes Windalia Sand Member|Overlies Birdrong Sandstone. Overlain by Windalia Radiolarite.|Argillaceous unit.|08-FEB-18
13315|Muderong Shale|67970|5|Briefly described|p4, p9, p10, pp13-14, p25 Fig.4.|Aptian|Hauterivian|Exmouth Plateau. Forms a regional seal.||Unit in Winning Group.|||Shallow marine mudstone.|
13315|Muderong Shale|68206|6|Mentioned|p30, 32-33|Barremian|Barremian|Carnarvon Basin. Appears as Munderong Shale on p32.||||Is overlain by Windalia Radiolarite.||
13315|Muderong Shale|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
13315|Muderong Shale|69182|5|Briefly described|Ch3 p8, Ch3 p12-p13|Cretaceous|Cretaceous|Carnarvon Basin. Deposited in a low-energy marine environment. At least 48m thick. Forms the regional seal for the Birdrong Sandstone. See also Ch3 p17-p20, Ch3 p23-p26, Ch3 p29, Ch3 p35, Ch3 p37, Ch3 p65, Ch3 p65-p66, Ch3 p69, Ch3 p71, Ch3 p73.||||Overlies the Birdrong Sandstone and the Mungaroo Formation. Overlain by the Windalia Radiolarite.|Shale.|
13315|Muderong Shale|69185|5|Briefly described|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|Of Northern Carnarvon Basin. Comprises southern part of the Winning Group.||Unit of Winning Group.||||
13315|Muderong Shale|69297|5|Briefly described|p247, p249, p251, p339|Barremian|Hauterivian|Southern Carnarvon Basin. Deposited during a marine transgressive cycle. Shales are potential hydrocarbon seals.||Winning Group|Includes the Windalia Sand Member.|Overlies the Birdrong Sandstone and unconformably overlies the Woodleigh Formation. Overlain by the Windalia Radiolarite.|Shale.|
13315|Muderong Shale|69558|6|Mentioned|p258 fig 419|Early Cretaceous|Early Cretaceous|||||Overlies the Birdrong Sandstone. Overlain by the Windalia Radiolarite. Faulted against the Wogatti Sandstone and the Gearle Siltstone.||25-MAY-21
13315|Muderong Shale|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Overlies Mardie Greensand (Upper Barrow Group), Forestier Claystone. Is overlain by Haycock Marl, Windalia Radiolarite.||
13315|Muderong Shale|70066|5|Briefly described|Dampier: Fig.2;p2-3. Exmouth: Fig.2;p1-3|Aptian|Valanginian|See also Regional: Fig.6; p6, p8-9. Northern Carnarvon Basin. Marine to marginal marine; glauconitic sandstone units host commercial oil accumulations in the Barrow Sub-basin. Provides a regional top-seal.||Winning Group.|Windalia Sand Member, M. australis Member, Mardie Greensand Member.|Overlies Birdrong Sandstone and Forestier Claystone. Is overlain by Windalia Radiolarite.||
13315|Muderong Shale|70906|5|Briefly described|p757-758, p764|Early Cretaceous|Early Cretaceous|Gorgon Platform. Appears as Muderong Formation on p760. Polygonal fault system described.|||Mardie Greensand Member.|Overlies Barrow Group. Is overlain by Windalia Radiolarite.||
13315|Muderong Shale|73564|5|Briefly described|p1225-1226, 1232, 1236|Cretaceous|Cretaceous|Exmouth Plateau. Appears also as Muderong Shale Formation (twice) on p1226.|||Mardie Greensand Member.|Overlies Birdrong Sandstone. Is overlain by Windalia Radiolarite.|Marine sediments.|
13325|Mudong Metamorphics|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Morrissey Metamorphic Suite.||||||
13325|Mudong Metamorphics|42260|6|Mentioned|p8|||Variation - Mudong Member previously published.||||||
13325|Mudong Metamorphics|72758|5|Briefly described|p11 Tb.1, p44-45.|||Previously named Mudong Member by Daniels (1970), (1st Edition Wyloo 1:250,000). Strongly deformed. Stratigraphic position uncertain. Here renamed Mudong Metamorphics with no stratigraphic connotation (p44-45), but shown p11 as part of Morrisey Metamorphic Suite p11 Table 1.|||||Quartzite, schist, amphibolite, and marble, locally migmatites.|
13341|Muja Coal Measures|14227|5|Briefly described|Enclos. 2|Permian|Permian|Overlies Premier Coal Measures. Geol. Prov: Collie Basin. Presented as Muja CM.||||||07-FEB-11
13341|Muja Coal Measures|22820|6|Mentioned|p21, p22|||Of the Collie Group. Geological province: Collie Basin.||||||12-AUG-08
13341|Muja Coal Measures|23174|5|Briefly described|Fig5p8|Late Permian|Late Permian|||||||
13341|Muja Coal Measures|42711|2|Defined|p5 Fig. 4, p27, Plates 2, 4, 5|Late Permian|Late Permian|Of Collie Group. Supersedes Muja Member and includes rocks from Cardiff Mbr and parts of Collieburn Mbr. Overlies Premier C.M. Thickness: ~450m. Geol.prov: Collie Basin. Contains 9 main coal seams with intercalated conglom/sst/siltst. Detailed lith.given||||||03-JUN-09
13341|Muja Coal Measures|43442|6|Mentioned|p50|||||||||
13341|Muja Coal Measures|64580|6|Mentioned|map legend|||Of Collie Group.||||||15-DEC-08
13341|Muja Coal Measures|64630|5|Briefly described|p31 Fig.2|Wordian|Roadian|Province: Collie Sub-basin. Overlies the Premier Coal Measures. Palynology age: D, ericianus to P. rugatus. Correlates with the base of the Williespe Formation.||||||23-JUL-13
13341|Muja Coal Measures|70097|5|Briefly described|p19 Fig.3|Wordian||Southern Perth Basin. Collie Sub-basin.||||Overlies Premier Coal Measures. Is overlain by Nakina Formation.|Includes coal.|12-SEP-17
13341|Muja Coal Measures|70774|5|Briefly described|p5 fig 3|Kazanian|Kazanian|Collie Basin.||||Unconformably? Overlies the Premier Coal Measures.||
13341|Muja Coal Measures|71146|6|Mentioned|p39 fig 31|||Perth Basin.|||||Coal seams.|
13341|Muja Coal Measures|72034|5|Briefly described|500k_interpgeop16_lut|Guadalupian|Kungurian|Perth Basin.  Age from biostratigraphy.||Collie Group.|||Interbedded poorly sorted feldspathic sandstone, carbonaceous shale, coal; conglomerate.|
13357|Mulgabbie Group|22534|6|Mentioned|p10|||Now abandoned||||||
13357|Mulgabbie Group|37373|5|Briefly described|Table 2.I|||||||||
13357|Mulgabbie Group|39869|6|Mentioned|Fig.2|||||||||
13357|Mulgabbie Group|41249|5|Briefly described|Table 1|||Mention P10||||||
13357|Mulgabbie Group|41370|5|Briefly described|p15|||||||||
13357|Mulgabbie Group|43075|5|Briefly described|Table 1|||||||||
13357|Mulgabbie Group|46416|6|Mentioned|p2|||||||||
13362|Mulgarra Sandstone|23529|5|Briefly described|p10|||Of the Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||28-JUL-08
13362|Mulgarra Sandstone|23589|5|Briefly described|p2 fig. 2|||Of Miningarra Subgroup. Underlain by Kulele Limestone. Geol. prov: Earaheedy Basin.||||||17-JUL-08
13362|Mulgarra Sandstone|23890|5|Briefly described|p21 Fig.11|||Of Miningara Subgroup. Geological Province: Earaheedy Basin.||||||
13362|Mulgarra Sandstone|24017|5|Briefly described|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
13362|Mulgarra Sandstone|24578|4|Described|p776 Fig.1, p781|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Overlies the Kulele Limestone. Geological Province: Earaheedy Basin.||||||07-NOV-08
13362|Mulgarra Sandstone|30010|6|Mentioned|p45|||||||||
13362|Mulgarra Sandstone|31217|2|Defined|p42|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
13362|Mulgarra Sandstone|36551|6|Mentioned|Table 29|||||||||
13362|Mulgarra Sandstone|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13362|Mulgarra Sandstone|37460|5|Briefly described|p143|||||||||
13362|Mulgarra Sandstone|38515|6|Mentioned|p9|||||||||
13362|Mulgarra Sandstone|38978|3|Fully described|p171|||||||||
13362|Mulgarra Sandstone|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13362|Mulgarra Sandstone|40355|5|Briefly described|p8|||||||||
13362|Mulgarra Sandstone|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13362|Mulgarra Sandstone|40938|2|Defined|p69|Paleoproterozoic|Paleoproterozoic|Mention p13.||||||07-NOV-08
13362|Mulgarra Sandstone|41997|6|Mentioned|Fig.2 P73|||||||||
13362|Mulgarra Sandstone|42548|5|Briefly described|p52|||||||||
13362|Mulgarra Sandstone|43595|5|Briefly described|Table 3-9,p346|||||||||
13362|Mulgarra Sandstone|50188|5|Briefly described|p2  Fig. 1, p3|||Of the Miningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Maximum Thickness: ~100m.||||||28-JUL-08
13362|Mulgarra Sandstone|50222|5|Briefly described|p320 Fig. 3, p329|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Sandstone, locally glauconitic, shale and minor carbonate. Max. thickness: ~100m. Age: 1.85Ga (Hallovic et al, 2004).  Geological Province: Earaheedy Basin.  See also p319 Fig. 2.||||||07-NOV-08
13362|Mulgarra Sandstone|50223|5|Briefly described|p345 Fig. 2, p348|Paleoproterozoic|Paleoproterozoic|Of the Miningarra Subgroup (Earaheedy Group). Sandstone, shale and minor carbonate rocks.  Max. thickness: 100m.  Geological Province:  Earaheedy Basin.  See also p355.||||||07-NOV-08
13362|Mulgarra Sandstone|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group).  Medium-grained quartz arenite; minor siltstone. Unconformably overlain by Bangemall Group. Max. thickness: ~100+m. Geological Province: Earaheedy Basin.||||||07-FEB-11
13362|Mulgarra Sandstone|50226|5|Briefly described|p423, p424 Fig. 5|||Top part of the Miningarra Subgroup (Earaheedy Group).  Geological Province: Earaheedy Basin.||||||09-DEC-04
13362|Mulgarra Sandstone|63866|4|Described|p166-p167|Orosirian|Orosirian|Eraheedy Basin.|1808 +/- 36 Ma (Halilovic et al, 2004)|Miningarra Subgroup||Overlies the Kulele Limestone.||
13362|Mulgarra Sandstone|64284|4|Described|p58 Fig. 1, p60 Fig. 2, p61|Paleoproterozoic|Paleoproterozoic|Of the Minningarra Subgroup (Earaheedy Group). Max. thickness: 100m. Geological Province: Earaheedy Basin. Sandstone, shale and minor carbonate.||||||07-FEB-11
13362|Mulgarra Sandstone|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Minningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. A molasse-type unit, recording the final influx of terrigenous sediments.||||||07-FEB-11
13362|Mulgarra Sandstone|64580|4|Described|map legend||Paleoproterozoic|Of Miningarra Subgroup. Sandstone; minor shale, limestone, and granule conglomerate; locally glauconitic.||||||09-DEC-08
13362|Mulgarra Sandstone|64725|6|Mentioned|p59.|||||Topmost unit in Miningarra Subgroup.||Overlies Kulele Limestone.||
13362|Mulgarra Sandstone|64772|4|Described|p12, Plate 1, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: c.1808Ma (SHRIMP, Halilovic et al 2004). Max. thickness: at least 100 m, not certain due to poor exposure. On Plate 1,  unit is of Earaheedy Group (as Miningarra Subgroup not shown). Geological province: Earaheedy Basin. Sandstone (usually glauconitic), shale and minor carbonate. See also p19 Fig.9, p20-21 Fig.10, p76-77 Fig.4.2, p79-81 App.4 Fig.4.3,||Of Miningarra Subgroup (top of Earaheedy Group)||Overlies Kulele Limestone|Sandstone (locally galuconitic), shale, and minor carbonate|25-NOV-13
13362|Mulgarra Sandstone|65472|5|Briefly described|p1, p3 Fig.2, p5 Fig. 4|||Thickness: ~100 m. Age: from Fig.2, after Pirajno et al. 2004. Earaheedy Basin. On p3 Fig.2, Miningarra Subgroup range not shown to include Kulele Limestone and Mulgarra Sandstone.|1.85 Ma detrital zircon U-Pb SHRIMP youngest age|Miningarra Subgroup||||
13362|Mulgarra Sandstone|65692|5|Briefly described|p9-11, p28, p55|||Is listed as [Mulgarra] Formation on p9. c.100m thick. Maximum depositional age: detrital zircons.|1808 +/- 36 Ma (Halilovic et al., 2004).|Miningarra Subgroup.||Overlies Kulele Limestone.|Sandstone, shale and carbonate.|
13362|Mulgarra Sandstone|66427|5|Briefly described|p43 Fig.2, p44 Tb.2, p46-51, p69-73|||c.100 m thick. Detrital zircon age from sandstone.|1808 +/- 36 Ma (U-Pb SHRIMP; Halilovic et al,2004)|Unit in Miningarra Subgroup.||Overlies Kulele Limestone.|Consists of fine-to-medium-grained, commonly glauconitic sandstone, shale and minor carbonate; local thin limestone beds, quartzose calcarenite horizons, and siltstone.|
13362|Mulgarra Sandstone|67855|6|Mentioned|p208 fig 3-8|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup||||
13362|Mulgarra Sandstone|68055|6|Mentioned|p77|Proterozoic|Proterozoic|Earaheedy Basin.||Miningarra Subgroup.||||
13362|Mulgarra Sandstone|69003|5|Briefly described|p13 Fig.17, p14-15|||Earaheedy Basin. c.100m thick. Detrital zircon maximum depositional age.|c.1808 Ma.|Miningarra Group.||Conformably? overlies Kulele Limestone.||
13362|Mulgarra Sandstone|69091|5|Briefly described|p181||Paleoproterozoic|Youngest unit in Earaheedy Basin. Detrital zircon maximum depositional age of ~1800 Ma (Halilovic et al., 2004).||||||
13362|Mulgarra Sandstone|69152|4|Described|1m_geologyp08_lut.csv|Orosirian|Orosirian|||Miningarra Subgroup|||Fine to medium grained quartz sandstone, locally glauconitic, shale and minor carbonate bands.|06-AUG-15
13362|Mulgarra Sandstone|69313|6|Mentioned|p22 Fig.4.2, p24-25|Statherian|Orosirian|This detrital zircon age is the basis for the maximum depositional age of the uppermost Earaheedy Group.|1808 +/- 36 Ma (SHRIMP U-Pb)|Minningarra Subgroup||Overlies the Kulele Limestone.|Sandstones.|08-SEP-17
13362|Mulgarra Sandstone|69596|6|Mentioned|p10-11|||Earaheedy Basin.||Miningarra Group.||||
13362|Mulgarra Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greensand, shale, crystalline carbonate, sandstone|
13362|Mulgarra Sandstone|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen. Of Earaheedy Basin.||Unit of Miningarra Group.|||Fine to medium grained quartz sandstone, locally glauconitic, shale and minor carbonate bands.|
13362|Mulgarra Sandstone|71484|4|Described|p124-125,132,137-138|Orosirian|Orosirian|Geological province: Of Earaheedy Basin. Thickness: ?200m maximum preserved thickness. Deposited in a coastal setting (muddy inner shelf with isolated sandy megaripples, through foreshore, beach and possibly tidal sandflat environments, to a washover lagoonal setting). Age constraint of c. 1800 Ma provided by Halilovic et al. (2004); 1867+\-25 Ma provided by Sheppard et al., 2016. Deposited prior to c. 1820 Ma Capricorn Orogeny along northern Yilgarn margin. May indicate the start of a compressional regime and Capricorn Orogeny, based on the change from carbonate deposition of the underlying Kulele Limestone to clastic deposition of this unit.||Unit of Miningarra Group.||Uppermost unit of Miningarra Group. Underlain by Kulele Limestone.|Fine- to medium-grained, commonly glauconitic sandstone, shale and minor carbonate.|30-AUG-19
13362|Mulgarra Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 1808+/-36 Ma, Min ~1650 Ma.|Miningarra Group|||Sandstone; minor shale, limestone, and granule conglomerate; locally glauconitic.|
13374|Mullaloo Sandstone Member|12759|4|Described|p43; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Eocene|Paleocene|Defined Quilty (1974). Type section in offshore Quinns Rock No.1 well, 20km W of Whitfords, (AMG Zone 50, 359480m E, 6480360m N) between 68-365 m depth. Max onshore thickness is 200m. Occupies deep marine channels incised into Kings Park Formation. Forms a minor confined aquifer.||At or near top of Kings Park Formation.|||Poorly sorted, fine- to very coarse-grained, pale brownish-green, slightly glauconitic and clayey sand.|12-MAY-14
13374|Mullaloo Sandstone Member|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Age: Early Eocene. Presented as Mullaloo Sandstone Mem.||||||07-FEB-11
13374|Mullaloo Sandstone Member|29693|6|Mentioned|Fig.7|||||||||
13374|Mullaloo Sandstone Member|31562|6|Mentioned|Fig. 3|||Member of Kings Park Formation.||||||15-JAN-08
13374|Mullaloo Sandstone Member|32748|2|Defined|p28|Tertiary|Tertiary|||||||
13374|Mullaloo Sandstone Member|32750|6|Mentioned|p307|||||||||
13374|Mullaloo Sandstone Member|34951|6|Mentioned|p115|||||||||
13374|Mullaloo Sandstone Member|36293|5|Briefly described|p197|||||||||
13374|Mullaloo Sandstone Member|44144|5|Briefly described|p503 Tb.4-21, p519|Early Eocene|Early Eocene|||Top of Kings Park Formation.|||Poorly sorted sandstone.|
13374|Mullaloo Sandstone Member|63745|5|Briefly described|p68, p78 Appx.|Eocene|Paleocene|At top of Kings Park Formation. Unconformably overlain by Perth Formation.||||||07-FEB-11
13374|Mullaloo Sandstone Member|68254|6|Mentioned|p1040 Tb.3|||Member status specified in heading of Table 3. See informal Mullaloo Sandstone in this paper.||||||
13374|Mullaloo Sandstone Member|68811|6|Mentioned|p180 tbl 39|Tertiary|Tertiary|||Of Kings Park Formation.||||15-APR-20
13392|Mulline Formation|41199|2|Defined|p8|Tertiary||Reserved as Mulline||||||
13392|Mulline Formation|50621|5|Briefly described|p159 Fig. 2|Cenozoic|Cenozoic|||||||19-NOV-08
13414|Munabia Sandstone|12729|6|Mentioned|p. 15; Figs. 4, 6, 24||Famennian|Replaced by the Munabia Formation due to greater shale proportion (Mory and Yasin, 1999).||||Conformably overlies the Gneudna Formation.|Sandstone and minor shale.|
13414|Munabia Sandstone|12731|5|Briefly described|p590 Fig.2.|Late Devonian|Late Devonian|||||Overlies Gneudna Formation.|Fine-grained, shallow marine to coastal siliciclastics.|
13414|Munabia Sandstone|12733|5|Briefly described|p554 Fig.2.|Late Devonian|Late Devonian|Frasnian-Famennian.||||Overlies Gneudna Formation. Is overlain by Willaradie Formation.|Clastics.|
13414|Munabia Sandstone|14227|5|Briefly described|Enclos. 2|||Presented as Munabia only - Sandstone inferred.||||||07-FEB-11
13414|Munabia Sandstone|22814|5|Briefly described|fig2|Devonian|Devonian|||||||
13414|Munabia Sandstone|23311|5|Briefly described|map legend|Famennian|Famennian|||||||
13414|Munabia Sandstone|23312|5|Briefly described|map legend|Famennian|Famennian|||||||
13414|Munabia Sandstone|23403|4|Described|p7|Early Carboniferous|Middle Devonian|Consists of well sorted, fine- to coarse-grained sandstone with minor siltstone and dolomite. Geological Province: Gascoyne Complex.||||||24-NOV-09
13414|Munabia Sandstone|23572|4|Described|p8 Fig. 6, p11|Frasnian|Frasnian|Geological Province: Carnarvon Basin. Underlying Unit: Gneudna Formation (conformable).||||||04-MAY-05
13414|Munabia Sandstone|23726|5|Briefly described|p33|Devonian|Devonian|Overlying unit Willaraddie Formation. Underlying unit Gneuda Formation. Geological Province: Carnarvon Basin.||||||
13414|Munabia Sandstone|23815|4|Described|p275, 276|Late Devonian|Late Devonian|Geological Province: Carnarvon Basin. Underlying unit: Gneudna Formation (conformable). Overlying unit: Willaraddie Formation (conformable). Max. thickness: 555 m. Contains lepidodendroid plants.||||||
13414|Munabia Sandstone|23935|5|Briefly described|p11 Fig.7|Famennian|Famennian|Conformably overlies Gneudna Formation. Geological Province: Southern Carnarvon Basin.||||||
13414|Munabia Sandstone|24059|5|Briefly described|p145|Late Devonian|Late Devonian|Geological Province: Carnarvon Basin.||||||
13414|Munabia Sandstone|24390|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
13414|Munabia Sandstone|30875|6|Mentioned|p10|||Devonian. See also P14||||||
13414|Munabia Sandstone|31561|5|Briefly described|p33|||See also P34. Late Devonian||||||
13414|Munabia Sandstone|32648|6|Mentioned|p32|||Frasnian - Famennian||||||
13414|Munabia Sandstone|32865|5|Briefly described|p477|||||||||
13414|Munabia Sandstone|33386|6|Mentioned|Fig.7|||||||||
13414|Munabia Sandstone|33453|5|Briefly described|p69|||||||||
13414|Munabia Sandstone|34484|6|Mentioned|Fig.1|||||||||
13414|Munabia Sandstone|35282|6|Mentioned|Fig.2|||||||||
13414|Munabia Sandstone|35981|6|Mentioned|p134|||||||||
13414|Munabia Sandstone|36257|6|Mentioned|Table 2.1|||||||||
13414|Munabia Sandstone|36743|6|Mentioned|p40|||||||||
13414|Munabia Sandstone|36890|3|Fully described|p276|||||||||
13414|Munabia Sandstone|36902|6|Mentioned|p22|||||||||
13414|Munabia Sandstone|38482|6|Mentioned|p22|||||||||
13414|Munabia Sandstone|38770|4|Described|p64|||||||||
13414|Munabia Sandstone|40617|6|Mentioned|Fig.1|||||||||
13414|Munabia Sandstone|40992|6|Mentioned|Fig.8|||||||||
13414|Munabia Sandstone|41271|3|Fully described|p50|||||||||
13414|Munabia Sandstone|41438|6|Mentioned|p102|||||||||
13414|Munabia Sandstone|41443|6|Mentioned|p159|||||||||
13414|Munabia Sandstone|41492|5|Briefly described|Fig.2|||||||||
13414|Munabia Sandstone|41512|6|Mentioned|p29|||||||||
13414|Munabia Sandstone|42030|3|Fully described|p744|||||||||
13414|Munabia Sandstone|42116|4|Described|p25|||||||||
13414|Munabia Sandstone|43566|6|Mentioned|p413|||||||||
13414|Munabia Sandstone|44344|14|Not recorded|p.5,7,22,24||Devonian|(G50-1). opp.4, map.||||||
13414|Munabia Sandstone|44345|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
13414|Munabia Sandstone|44537|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
13414|Munabia Sandstone|44657|14|Not recorded|p.5,7,8,17|||||||||
13414|Munabia Sandstone|45015|2|Defined|p49-54, map legend|Famennian|Frasnian|Quartz sandstone with a member of siltstone, quartzwacke and limestone in the upper part. Conformably overlies Gneudna Fm; conformably overlain by Willaraddie Fm., unconformably by Austin Greywacke, disconf. by Moogooree Limestone. Max. thick: 4450ft.||||||31-MAY-06
13414|Munabia Sandstone|45016|14|Not recorded|p.9,21,24||Devonian|||||||
13414|Munabia Sandstone|45041|6|Mentioned|Fig.45|||Frasnian - Famennian||||||
13414|Munabia Sandstone|45063|6|Mentioned|p30|||See also Fig. 9. Dev.||||||
13414|Munabia Sandstone|50085|5|Briefly described|p19 Fig. 10|Late Devonian|Late Devonian|Geological Province: Southern Carnarvon Basin.||||||
13414|Munabia Sandstone|60384|5|Briefly described|p244|Late Devonian|Late Devonian|Southern Carnarvon Basin. See also Munabia Formation. Described along with Willaraddie Formation as: coastal to nearshore sandstone with lesser claystone, conglomerate and dolomite.||||?Overlies Gneudna Formation. Probably lateral equivalent to Willaraddie Formation.||
13414|Munabia Sandstone|60725|5|Briefly described|p29 Fig.2; p30; p33,p35-36 Figs.4,5,6. |Famennian|Famennian|||||||
13414|Munabia Sandstone|61563|6|Mentioned|p578|||See also p579 Fig. 3.||||||15-DEC-05
13414|Munabia Sandstone|61958|5|Briefly described|Map sheet 1|Devonian|Devonian|||||||
13414|Munabia Sandstone|64580|6|Mentioned|map legend|||Devonian succession, Southern Carnarvon Basin.||||||15-DEC-08
13414|Munabia Sandstone|67200|5|Briefly described|p7 fig 5, |Devonian|Devonian|Alternate name for Munabia Formation?||||Overlies Gneudna Formation, overlain by Willaraddie Formation|Trough and planar cross bedded, medium grained sandstone with common flaser siltstone beds.|
13414|Munabia Sandstone|68297|5|Briefly described|p183|Frasnian|Frasnian|Carnarvon Basin, WA. Includes Bothreolepis fauna||||Conformably overlies Gneudna Formation||
13414|Munabia Sandstone|68298|5|Briefly described|p233|||Carnarvon Basin. Fragmentary fauna of 3 taxa (Appendix 1).||||Overlies Gneudna Formation.||
13414|Munabia Sandstone|69011|5|Briefly described|Map Legend|Devonian|Devonian|Southern Carnarvon Basin.||||Overlain by the Willaraddie Formation. Underlain by the Gneudna Formation.|Comprises medium-grained quartz sandstone; minor siltstone, conglomerate, and dolomite.|
13414|Munabia Sandstone|69029|6|Mentioned|p326,328|Famennian|Frasnian|Of onshore Carnarvon Basin.||||Overlain by Willaradie Formation. Underlain by Gneudna Formation.||
13414|Munabia Sandstone|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Late Devonian|Late Devonian|Carnarvon Basin. Deposited in a barrier complex. Incorrectly referred to as the Munabia Formation in Ch3 p10. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Conformably overlies (or interfingers with) the Gneudna Formation. Overlain by the Willaraddie Formation.|Sandstone with minor claystone, conglomerate and dolomite.|
13414|Munabia Sandstone|69297|5|Briefly described|p249|Famennian|Frasnian|Gascoyne Sub-basin of the Southern Carnarvon Basin.||||Overlies the Gneudna Formation. Overlain by the Moogooree Limestone.|Sandstones.|
13414|Munabia Sandstone|70127|5|Briefly described|Map legend|Devonian|Devonian|Southern Carnarvon Basin.|||||Medium-grained quartz sandstone; minor siltstone, conglomerate and dolomite.|
13414|Munabia Sandstone|70138|5|Briefly described|Map legend.|Devonian|Devonian|Southern Carnarvon Basin.||||Overlies Gneudna Formation. Is overlain by Willaraddie Formation.|Medium-grained quartz sandstone; minor siltstone, conglomerate and dolomite.|
13414|Munabia Sandstone|70795|4|Described|100k_geologyp_lut.csv|Famennian|Famennian|Also 100k_interpgeop_lut.csv|372-359 Ma||||Medium-grained quartz sandstone; minor siltstone, conglomerate, and dolomite.|
13414|Munabia Sandstone|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|||||||
13414|Munabia Sandstone|71146|5|Briefly described|p6|Famennian|Frasnian|Southern Carnarvon Basin.||||Overlies the Gneudna Formation. Overlain by the Willaraddie Formation.|Sandstone.|
13414|Munabia Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone, limestone|
13419|Mundabia Sandstone|35282|6|Mentioned|Fig.19|||||||||
13423|Mundarie Siltstone|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Of the Lyons Group. Underlying unit: Koomberan Greywacke. Overlying unit: Thambrong Formation.||||||
13423|Mundarie Siltstone|32648|6|Mentioned|p32|||Lyons Group||||||
13423|Mundarie Siltstone|36890|6|Mentioned|p279|||||||||
13423|Mundarie Siltstone|37295|6|Mentioned|Table 2|||||||||
13423|Mundarie Siltstone|41271|6|Mentioned|p65|||||||||
13423|Mundarie Siltstone|44344|14|Not recorded|p.6,8-9,24,opp.4,map||Sakmarian|Sakmarian in age. (G50-1).||||||
13423|Mundarie Siltstone|44345|14|Not recorded|map legend||Sakmarian|Sakmarian.||||||
13423|Mundarie Siltstone|44532|4|Described|p.5, map|||(G50-5).||||||
13423|Mundarie Siltstone|44533|5|Briefly described|map legend||Sakmarian|Sakmarian.||||||
13423|Mundarie Siltstone|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group.||||||01-JUN-06
13423|Mundarie Siltstone|45016|2|Defined|p40-47||Sakmarian|Tb, p7,12,13,16,36,38,60,67,104, Fg. 52,56. (F50-13). Defn on Tech File G/50-1.||||||
13423|Mundarie Siltstone|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
13455|Mungadan Sandstone|14228|6|Mentioned|p8|Permian|Permian|||Kennedy Group||||
13455|Mungadan Sandstone|23174|5|Briefly described|Fig5p8||Late Permian|||||||
13455|Mungadan Sandstone|23311|5|Briefly described|map legend|Paleozoic|Paleozoic|Of Kennedy Group.||||||07-NOV-08
13455|Mungadan Sandstone|23312|5|Briefly described|map legend|||Of Kennedy Group.||||||
13455|Mungadan Sandstone|23403|4|Described|p8|Late Permian|Early Permian|Of Kennedy Group.||||||24-NOV-09
13455|Mungadan Sandstone|23726|4|Described|p54|Permian|Permian|Of Kennedy Group. Overlying unit Binthalya Formation. Underlying unit Coolkilya Sandstone. Geological Province: Carnarvon Basin.||||||
13455|Mungadan Sandstone|23815|4|Described|p289|Kungurian|Kungurian|Geological Province: Carnarvon Basin. Of the Kennedy Group. Overlying unit: Binthalya Formation (conformable). Underlying unit: Coolkilya Greywacke. Max. thickness: 61 m. Fossils are serpulids and very rare bivalves.||||||
13455|Mungadan Sandstone|24044|3|Fully described|p542|Permian|Carboniferous|Of Kennedy Group.  Geological Province: Merlinleigh Sub-basin. Maximum thickness: 116m.||||||
13455|Mungadan Sandstone|30545|6|Mentioned|Fig.2|||Kazanian||||||
13455|Mungadan Sandstone|31561|6|Mentioned|p7|||Conformable on Coolkilya Greywacke.||||||06-DEC-06
13455|Mungadan Sandstone|32648|6|Mentioned|p32|||Kennedy Gp.||||||
13455|Mungadan Sandstone|33701|6|Mentioned|Fig.1|||Kazanian & Kungurian.||||||
13455|Mungadan Sandstone|33710|6|Mentioned|Fig.1|||||||||
13455|Mungadan Sandstone|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
13455|Mungadan Sandstone|34532|6|Mentioned|p225|||Kennedy Gp.||||||
13455|Mungadan Sandstone|35282|6|Mentioned|p39|||||||||
13455|Mungadan Sandstone|36257|6|Mentioned|Table 2.1|||||||||
13455|Mungadan Sandstone|36890|3|Fully described|p288|||||||||
13455|Mungadan Sandstone|37295|6|Mentioned|Table 2|||||||||
13455|Mungadan Sandstone|37303|5|Briefly described|p65|||||||||
13455|Mungadan Sandstone|39316|6|Mentioned|Fig.2|||||||||
13455|Mungadan Sandstone|39974|6|Mentioned|Fig.1|||||||||
13455|Mungadan Sandstone|40617|6|Mentioned|Fig.1|||||||||
13455|Mungadan Sandstone|41271|3|Fully described|p103|||||||||
13455|Mungadan Sandstone|41438|6|Mentioned|p105|||See also Fig.11||||||
13455|Mungadan Sandstone|41632|6|Mentioned|p1|||||||||
13455|Mungadan Sandstone|42116|5|Briefly described|p28|||||||||
13455|Mungadan Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
13455|Mungadan Sandstone|44219|14|Not recorded|p31||Kazanian|pt. of Kennedy Group.||||||
13455|Mungadan Sandstone|44344|14|Not recorded|p.16, opp.4, map||Kungurian|Kungurian; fm. of Kennedy Group. (G50-1).||||||
13455|Mungadan Sandstone|44345|14|Not recorded|map legend||Kungurian|Kungurian.||||||
13455|Mungadan Sandstone|44537|14|Not recorded|map legend||Artinskian|||||||
13455|Mungadan Sandstone|44657|14|Not recorded|p.5,6,10|||||||||
13455|Mungadan Sandstone|45015|5|Briefly described|map legend|Kungurian|Kungurian|Of the Kennedy Group.||||||01-JUN-06
13455|Mungadan Sandstone|45016|2|Defined|p.186-8||Kungurian|Tb, p.171,176,178,181,182,185. ?Kungurian. (G50-1).||||||
13455|Mungadan Sandstone|48610|14|Not recorded|Pl.1|||||||||
13455|Mungadan Sandstone|48858|14|Not recorded|p.5,6||Kungurian|Kungurian. (G50-1/Norton).||||||
13455|Mungadan Sandstone|49644|5|Briefly described|Table|||||||||
13455|Mungadan Sandstone|50620|5|Briefly described|p191|Late Permian|Late Permian|Of the Kennedy Group. Geological Province: Carnarvon Basin.||||||
13455|Mungadan Sandstone|61958|5|Briefly described|Map sheet 1|Kungurian|Kungurian|Of the Kennedy Group.||||||
13455|Mungadan Sandstone|64580|6|Mentioned|map legend|||Of Kennedy Group.||||||15-DEC-08
13455|Mungadan Sandstone|66189|4|Described|p453-454, p459, p463, Fig 2,56|Guadalupian|Guadalupian|Of the Kennedy Group. Overlies Coolkilya Sandstone, underlies Binthalya Formation. Interbedded brown to reddish-brown sandstone and siltstone, rich in fossils of Paleodictyon ichnospecies. Near-shore facies and fossils, with periodic tidal invasions.||||||
13455|Mungadan Sandstone|67200|5|Briefly described|p7 fig 5,|Permian|Permian|||Kennedy Group||Overlies Coolkilya Sandstone, overlain by Binthalya Sandstone|Bioturbated,parallel bedded, interbedded,  sandstone and siltstone.|
13455|Mungadan Sandstone|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Kennedy Group.|||Comprises fine- to coarse-grained sandstone, minor siltstone.|
13455|Mungadan Sandstone|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||||||
13455|Mungadan Sandstone|70795|4|Described|100k_geologyp_lut.csv|Guadalupian|Guadalupian|Also 100k_interpgeop_lut.csv|272-260 Ma|Kennedy Group|||Fine- to coarse-grained sandstone, minor siltstone.|
13455|Mungadan Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, sandstone|
13455|Mungadan Sandstone|72505|5|Briefly described|p890|Wordian|Roadian|Southern Carnarvon Basin. Correlates with the Microbaculispora villosa zone and the Dulhuntyispora granulata zone.||Kennedy Group||Overlies the Coolkillya Sandstone. Overlain by the Binthalya Formation.||
13455|Mungadan Sandstone|72910|4|Described|p4, p6, p17-20, p25, p34, p38, p41.|Roadian|Kungurian|Thickness max 116m. Type section located at East side, Wandagee Hill, 23d50m10sS; 114d25m50sE. Age shown as Ufimian. Fluvial dominated. Represents renewed deltaic progradation.||Kennedy Group||Conformably overlies Coolkilya Sandstone and underlies Binthalya Formation.|Pale coloured fine to coarse sandstone with minor siltstone.|
13459|Mungari Monzogranite|23786|5|Briefly described|p34 Tb. 4|||Geological Province: Yilgarn Craton.||||||
13459|Mungari Monzogranite|41786|6|Mentioned|p334|||||||||
13459|Mungari Monzogranite|42221|6|Mentioned|p30|||||||||
13459|Mungari Monzogranite|42697|5|Briefly described|map legend|||||||||
13459|Mungari Monzogranite|42892|3|Fully described|p46|||age of 2620 +/- 20 Ma||||||
13459|Mungari Monzogranite|43102|5|Briefly described|Fig.2|||||||||
13459|Mungari Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||11-JUN-15
13459|Mungari Monzogranite|43496|6|Mentioned|15|||Age: 2610Ma||||||
13459|Mungari Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmmu]   Medium-grained, equigranular, two-mica monzogranite; massive.||||||
13459|Mungari Monzogranite|65204|5|Briefly described|p18, p19 Tbl.4,|Neoarchean||U-Pb zircon age 2602+/-11 Ma; 1-3mm grains; equigranular||||||11-JUN-15
13459|Mungari Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium-grained, equigranular, biotite-muscovite monzogranite; massive.||||||07-FEB-11
13459|Mungari Monzogranite|68289|5|Briefly described|p16|||Intrudes unnamed felsic volcaniclastic rocks. This unit is an ovoid body 4km wide and 8km long. Belongs to the low CA group of Cassidy et al (2002).||||Intrudes the Black Flag Group.|Medium-grained and mainly equigranular monzogranite with scattered subhedral to anhedral zoned feldspars.|
13459|Mungari Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton. Migrated from OZCHRON1. Original comment: 'pluton age of 2602+/-11'. from OZCHRON1. Original comment: 'inheritance age: ~2810 Ma.|2600+/-12 Ma U/Pb SHRIMP||||Medium-grained, equigranular, biotite-muscovite monzogranite; massive.|06-AUG-15
13459|Mungari Monzogranite|69631|5|Briefly described|p18-20|||A well-exposed, ovoid body, 4x8 km, at Mungari, c.12km NE of Coolgardie. Post-tectonic intrusion. No SHRIMP dating; age estimated to be younger than c.2660 Ma (Cassidy et al., 2002).||||Intrudes Black Flag Group.|Medium-grained, mainly equigranular, low-Ca monzogranite; has a broad aureole to the S.|
13459|Mungari Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|See also GA_rocks.csv, and GA_geochron.csv where two other age determinations given are 2603 +/- 19 Ma and 2600 +/- 12 Ma (both SHRIMP).|2640 +/- 25 Ma (isotopic) - 2600 Ma (inferred).||||Medium-grained, locally very sparsely feldspar-porphyritic, equigranular, biotite-muscovite monzogranite; massive.|
13459|Mungari Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
13459|Mungari 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.|2642+\-25 Ma; 2600 Ma||||Medium-grained, equigranular, biotite--muscovite monzogranite; massive|
13459|Mungari Monzogranite|73391|6|Mentioned|p22, 100, 102-103, Appendices.|||Kalgoorlie district. Late to post-tectonic intrusion. Muscovite-bioite schists occur in the metamorphic aureole.||||||
13466|Mungaroo Formation|6876|6|Mentioned|p100 Fig.5.|Triassic|Triassic|||||||
13466|Mungaroo Formation|7142|6|Mentioned|p355.|||Northern Carnarvon Basin. Chronostratigraphically equivalent to a predominantly sandy succession with basal limestone, and shale interbeds, that overlies the Locker Shale in the Browse Basin.||||||
13466|Mungaroo Formation|12466|5|Briefly described|p178.|Late Triassic|Late Triassic|Contains Leatherback 1 accumulation, the first discovery of oil along the eastern margin of the Carnarvon Basin. Sealed by Dingo Claystone, the possible source with near-shore and more terrigenous facies. Deposited in fluvial to deltaic environments. Lean in organic matter and have only poor to fair hydrocarbon source potential.||||Overlies Locker Shale. Overlain by Dingo Claystone.|Sandstone, minor claystone interbeds.|22-FEB-13
13466|Mungaroo Formation|12471|5|Briefly described|p475 Fig.2, p476.|Late Triassic|Middle Triassic|Major delta lobes prograded across the Peedamullah Shelf depositing sand, mud and coal. Sandstones have good hydrocarbon reservoir properties.||||Overlies Locker Shale. Is overlain by Muderong Shale.|Dominantly argillaceous, with sandstone and coal.|27-OCT-14
13466|Mungaroo Formation|12491|6|Mentioned|p453, p454 Fig.7, p456 Fig.9|||Fluvio-deltaic to marginal marine sediments.||||Is overlain by Brigadier Formation and Murat Formation.||06-NOV-14
13466|Mungaroo Formation|12498|5|Briefly described|p517 Fig.3. |Late Triassic|Late Triassic|North of Dampier Sub-basin. Carbonaceous units are considered a prime hydrocarbon source of Lambert Deep prospect.||||Is overlain by Brigadier Formation.|Delta plain facies including carbonaceous claystones and coals.|
13466|Mungaroo Formation|12758|6|Mentioned|p16|||Of the Barrow-Dampier Sub-basin.  Correlates with the Myalup Member (Lesueur Sandstone).  Geological Province:  Northern Carnarvon Basin.||||||
13466|Mungaroo Formation|13615|3|Fully described|p3-5, p6-8, p12, 13, 17, 18, 27,|Toarcian|Ladinian|Peedamullah Shelf. Up to 1030m thick onshore reaches more than 3000m thick offshore. Spores/Pollen Zone and Dinoflagellate zones provided. Deposited as a regressive fluviodeltaic complex. Porosity of this unit is provided. Intersected in numerous drillholes. In the Tubridgi Gasfield hosts 11% of the gas reserves. See also p29-30, p35, p38-40, p43-44, p47, p51-52, p55-56, p58-59, p65-71, p75, p78-86, p88, p102 App. 3, Plates 2, 3.|c. 235 Ma|||Conformably overlies the Locker Shale. Conformably overlain by the Dingo Claystone. Unconformably overlain by the Muderong Shale and the Flacourt Formation.|Medium-grained, moderately sorted quartzose sandstone to conglomerate.|09-FEB-19
13466|Mungaroo Formation|22702|5|Briefly described|p105||Middle Triassic|||||||
13466|Mungaroo Formation|22703|4|Described|p117,118,Fig.3|Norian|Scythian|||||||
13466|Mungaroo Formation|23355|5|Briefly described|7|Triassic|Triassic|||||||
13466|Mungaroo Formation|23356|5|Briefly described|26 Tab.2|Early Jurassic|Late Triassic|||||||
13466|Mungaroo Formation|23359|5|Briefly described|79 Tab.2|Triassic|Triassic|||||||
13466|Mungaroo Formation|23379|5|Briefly described|p173||Late Triassic|of Barrow Sub-basin, Carnarvon Basin.||||||
13466|Mungaroo Formation|23726|5|Briefly described|p8 Fig 2c|Late Triassic|Middle Triassic|Overlying unit Murat Siltstone. Underlying unit Locker Shale. Geological Province: Carnarvon Basin.||||||06-DEC-06
13466|Mungaroo Formation|23815|4|Described|p289, 291|Late Triassic|Middle Triassic|Formerly known as the "Mungaroo Beds". Geological Province: Carnarvon Basin. Underlying unit: Locker Shale (conformable). Overlying unit: Birdrong Sandstone (unconformable). Max thickness: 1249 m.||||||27-APR-05
13466|Mungaroo Formation|24060|5|Briefly described|p159|Late Triassic|Middle Triassic|Geological Province: Dampier Sub-basin.||||||
13466|Mungaroo Formation|24084|5|Briefly described|p146 Fig.2|Triassic|Triassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
13466|Mungaroo Formation|24205|5|Briefly described|p248, p253|Triassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||
13466|Mungaroo Formation|24208|5|Briefly described|p174|Late Triassic|Late Triassic|Fluvio-deltaic sands.  Geological Province:  Dampier Sub-basin (Carnarvon Basin).||||||
13466|Mungaroo Formation|24246|5|Briefly described|p18, 19|Late Triassic|Late Triassic|Geological Province: Carnarvon Basin.||||||
13466|Mungaroo Formation|24331|5|Briefly described|p475 Fig.2|Late Triassic|Early Triassic|Conformably overlies Locker Shale. Overlain by Brigadier Formation (conformable) and Dingo Claystone (unconformable). Fluvial to marginal marine. Geological Province: Barrow Sub-basin.||||||
13466|Mungaroo Formation|24351|5|Briefly described|Plate 4 (in pocket)|Early Jurassic|Triassic|Geological Province: Exmouth Plateau and Exmouth Sub-basin.||||||13-DEC-07
13466|Mungaroo Formation|24390|5|Briefly described|p22|Late Jurassic|Late Triassic|Geological Province: Northern Carnarvon Basin.||||||
13466|Mungaroo Formation|24409|5|Briefly described|p48|Ladinian|Ladinian|Fluvio-deltaic siliclastics. Thickness: 5-6km. Geological Province: Carnarvon Basin||||||01-SEP-08
13466|Mungaroo Formation|30265|6|Mentioned|p89|||Main gas-bearing formation on the Ranklin Shelf.||||||
13466|Mungaroo Formation|30624|6|Mentioned|p1853|||||||||
13466|Mungaroo Formation|30625|6|Mentioned|p2115|||Eaglehawk flows up to 1,645 b/d. Upper Triassic||||||
13466|Mungaroo Formation|30693|6|Mentioned|p50|||||||||
13466|Mungaroo Formation|31898|6|Mentioned|p31|||||||||
13466|Mungaroo Formation|32642|6|Mentioned|p77|||Reservoir characteristics.||||||
13466|Mungaroo Formation|32648|6|Mentioned|p32|||Triassic||||||
13466|Mungaroo Formation|34846|6|Mentioned|Fig.3|||||||||
13466|Mungaroo Formation|35983|6|Mentioned|Table 27|||||||||
13466|Mungaroo Formation|36112|5|Briefly described|p27|||||||||
13466|Mungaroo Formation|36257|6|Mentioned|Table 2.1|||||||||
13466|Mungaroo Formation|36266|6|Mentioned|p152|||||||||
13466|Mungaroo Formation|36890|3|Fully described|p291|||Formerly Mungaroo Beds||||||
13466|Mungaroo Formation|37065|5|Briefly described|p38|||||||||
13466|Mungaroo Formation|37577|6|Mentioned|p78|||||||||
13466|Mungaroo Formation|37685|6|Mentioned|p6|||||||||
13466|Mungaroo Formation|37688|6|Mentioned|p16|||||||||
13466|Mungaroo Formation|38655|6|Mentioned|p10|||||||||
13466|Mungaroo Formation|38732|6|Mentioned|p31|||||||||
13466|Mungaroo Formation|39427|4|Described|Table 1|||||||||
13466|Mungaroo Formation|39757|6|Mentioned|p1605|||||||||
13466|Mungaroo Formation|40306|6|Mentioned|p58|||||||||
13466|Mungaroo Formation|40617|6|Mentioned|p7|||||||||
13466|Mungaroo Formation|40897|6|Mentioned|p152|||||||||
13466|Mungaroo Formation|40992|6|Mentioned|Fig.8|||||||||
13466|Mungaroo Formation|41170|6|Mentioned|Fig.3|||||||||
13466|Mungaroo Formation|41271|3|Fully described|p113|||||||||
13466|Mungaroo Formation|41436|6|Mentioned|p44|||||||||
13466|Mungaroo Formation|41438|4|Described|p106|||||||||
13466|Mungaroo Formation|41439|5|Briefly described|p120|||||||||
13466|Mungaroo Formation|41440|4|Described|p136|||||||||
13466|Mungaroo Formation|41441|5|Briefly described|p152|||||||||
13466|Mungaroo Formation|41443|4|Described|p164|||||||||
13466|Mungaroo Formation|41444|4|Described|p179|||||||||
13466|Mungaroo Formation|41446|6|Mentioned|Fig.17|||||||||
13466|Mungaroo Formation|41447|6|Mentioned|Fig.3|||||||||
13466|Mungaroo Formation|41712|6|Mentioned|p279|||||||||
13466|Mungaroo Formation|41716|5|Briefly described|p334|||||||||
13466|Mungaroo Formation|41732|6|Mentioned|p534|||See also P538||||||
13466|Mungaroo Formation|42062|5|Briefly described|p27|||||||||
13466|Mungaroo Formation|42075|5|Briefly described|Fig.4 P245|||||||||
13466|Mungaroo Formation|42116|5|Briefly described|Fig.1 P6|||||||||
13466|Mungaroo Formation|42395|6|Mentioned|p80|||||||||
13466|Mungaroo Formation|42463|6|Mentioned|Fig.2 P169|||||||||
13466|Mungaroo Formation|42615|5|Briefly described|p27, p6|||||||||
13466|Mungaroo Formation|43600|5|Briefly described|p242|||||||||
13466|Mungaroo Formation|43705|6|Mentioned|p14||Triassic|||||||
13466|Mungaroo Formation|43712|5|Briefly described|p10|||||||||
13466|Mungaroo Formation|43722|5|Briefly described|p9||Late Triassic|||||||
13466|Mungaroo Formation|43724|5|Briefly described|p28||Late Triassic|||||||
13466|Mungaroo Formation|43825|6|Mentioned|p145||Triassic|||||||
13466|Mungaroo Formation|43826|6|Mentioned|Fig.2,p163|Late Triassic|Middle Triassic|||||||01-MAR-10
13466|Mungaroo Formation|43827|6|Mentioned|p195|||||||||
13466|Mungaroo Formation|44143|5|Briefly described|p447|Triassic|Triassic|Carnarvon Basin. Is equivalent to Keraudren Formation of the Canning Basin.||||||23-NOV-17
13466|Mungaroo Formation|44937|5|Briefly described|p95,99-100|Early Jurassic|Late Triassic|||||||
13466|Mungaroo Formation|45142|6|Mentioned|p8|||||||||
13466|Mungaroo Formation|46950|6|Mentioned|Fig.15|||||||||
13466|Mungaroo Formation|49942|5|Briefly described|p10|Triassic|Triassic|Equivalent to Lesueur Sandstone. Geological Province: North Carnarvon Basin.||||||
13466|Mungaroo Formation|50024|5|Briefly described|p13|Late Triassic|Late Triassic|Hosts recoverable oil.  Geological Province: Carnarvon Basin.||||||
13466|Mungaroo Formation|50025|5|Briefly described|p12|Triassic|Triassic|Contains sandstone oil reservoirs sealed by Dingo Claystone.  Geological Province: Exmouth Sub-basin.||||||
13466|Mungaroo Formation|50085|5|Briefly described|p23 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin.||||||
13466|Mungaroo Formation|60379|6|Mentioned|p126 fig 3, p136|Carnian|Norian|Dampier sub-basin, Carnarvon Basin||||||
13466|Mungaroo Formation|60384|6|Mentioned|p243 Fig 2b|Late Triassic|Middle Triassic|Northern Carnarvon Basin.||||||
13466|Mungaroo Formation|60386|6|Mentioned|p300|Late Triassic|Early Triassic|Northern Carnarvon Basin. Non-marine.||||||
13466|Mungaroo Formation|60725|6|Mentioned|p33 Fig.4, p35 Fig.5, p36 Fig.6. |Triassic|Triassic|||||||
13466|Mungaroo Formation|61023|5|Briefly described|p27 Fig. 12|Triassic|Triassic|Geological Province: Northern Carnarvon Basin. See also p29.||||||11-APR-08
13466|Mungaroo Formation|62734|6|Mentioned|p1362 Fig. 2|||Geological Province: Barrow Sub-basin.||||||01-SEP-08
13466|Mungaroo Formation|62837|5|Briefly described|Stratigraphic columns|Late Triassic|Late Triassic|Age: 230-205Ma. Geological Province: Northern Carnarvon Basin.||||||01-MAR-10
13466|Mungaroo Formation|63929|6|Mentioned|p131 Fig.2.|Triassic|Triassic|Barrow Sub-basin, Peedamullah Shelf, Wombat Plateau, Rowley Terrace. Predominantly non-marine clastic sediments.||||Overlies Locker Shale. Is overlain by Brigadier Formation.||
13466|Mungaroo Formation|63936|4|Described|p181, p184-186, p191|Triassic|Triassic|Formalised as Mungaroo Formation by Playford et al. (1975). Previously Mungaroo Beds (Parry, in Jones (1967), whose type section was the interval 749-1992m in Long Island 1. Redefined here to the interval 808-1992m. Northern Carnarvon Basin. Palynofacies and palynological zones detailed. Swamp, brackish/marginal marine, to channel deposits.|||Is overlain by Brigadier Formation.||Mainly blocky sandstone beds separated by thin claystone intervals.|
13466|Mungaroo Formation|63950|5|Briefly described|p336 Fig. 4, p334|Late Triassic|Middle Triassic|Overlies Locker Shale; underlies Brigadier Formation. Geological Province: northern Carnarvon Basin. Characterised by interbedded sandstone and claystone sequence; fluvio-deltaic deposits. detailed lithology included (p343). See also p334, p335.||||||27-MAY-08
13466|Mungaroo Formation|64977|6|Mentioned|p493 Fig.3.|Late Triassic|Early Triassic|Thevenard Island area.||||Overlies Locker Shale. Is unconformably overlain by Dingo Claystone.||
13466|Mungaroo Formation|64978|6|Mentioned|p528 Fig.2.|Late Triassic|Late Triassic|||||||
13466|Mungaroo Formation|65078|5|Briefly described|p35 Fig. 11|Triassic|Triassic|Geological province: Barrow Sub-basin.||||||
13466|Mungaroo Formation|65708|5|Briefly described|p107|Early Triassic|Early Triassic|North West Shelf. An important reservoir; supplied by Jurassic-Triassic source rocks (Locker Formation and Dingo Claystone).|||||Deltaic-marine sandstones.|29-JUN-22
13466|Mungaroo Formation|66124|5|Briefly described|p169, p170 Fig.2|Rhaetian|Anisian|Non-marine. Overlies Locker Shale and underlies Brigadier Formation. Canning Basin, Wombat Plateau and Rowley Terrace.||||||
13466|Mungaroo Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes grey mottled siltstone; pale grey/buff sandstone.|
13466|Mungaroo Formation|67200|5|Briefly described|p8 fig 6, p48, p54, app 2 p7|Triassic|Triassic|Thermal conductivity of 2.39 W/mK||||Overlies Locker Shale, overlain by Brigadier Formation, Murat Siltstone|Interbedded sandstone and mottled siltstone.|
13466|Mungaroo Formation|67368|5|Briefly described|p209 Fig.4, p210 Fig.5, p212, p217.|Late Triassic|Middle Triassic|Gas reservoir for Pemberton Field. Is juxtaposed, across the major North Rankin Field bounding fault, against the Legendre Formation.||||Is overlain by Brigadier Formation.||
13466|Mungaroo Formation|67369|4|Described|p245, p246 Fig.3, p247, p253, pp259-262.|Norian|Late Triassic|Dampier Sub-basin. Interpreted as a fluvio-deltaic system which is described in detail; amalgamated fluvial incised valley sandstones within floodplain shales, in a broad, low relief coastal to alluvial plain. Gross sediment transport direction was from east to west. Contains excellent gas-bearing sands in the Pluto (average net porosity of 28% and average gas saturation of 93% for the Lower E Unit) and Xena Gas Fields. The change to marine conditions of the Brigadier Formation from this fluvial unit is marked by A. reducta marker horizon.||||Is overlain by Brigadier Formation.|Unconsoliated, planar cross-bedded, fining-upwards packages of medium- to coarse-grained sandstone; silty sandstone; black shales with bioturbation, root traces and paleosol horizons; minor coaly material.|
13466|Mungaroo Formation|67970|5|Briefly described|p3, pp5-7, p9, p10, pp13-14, p25 Fig.4.|Rhaetian|Anisian|Exmouth Plateau hydrocarbon source and reservoir: gas-prone. Gas was found by Hess in its Briseis 1 well in this unit and in the post-Callovian section; other companies' wells have also intersected gas plays. c.380 m thick. (Fluvio-deltaic) sandstone porosity decreases with depth. Has intraformational seals.||||Overlies conformably, and grades into, Locker Shale. Is overlain by Brigadier Formation.|Interbedded sandstone, siltstone, carbonaceous claystone; minor coal and dolomite.|
13466|Mungaroo Formation|68054|6|Mentioned|p43|Late Triassic|Late Triassic|Northern Carnarvon Basin. The base of the Perseus-3A well, at a total depth of 3915m.||||||
13466|Mungaroo Formation|69029|6|Mentioned|p328|Triassic|Triassic|Of Canning Basin.||||||
13466|Mungaroo Formation|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|Triassic|Triassic|Carnarvon Basin. Exhibits good porosity and permeability. A regressive unit deposited in a fluvio-deltaic setting; sandstones show high porosity and permeability. See also Ch3 p15, Ch3 p17-p18, Ch3 p23, Ch3 p27, Ch3 p29-p30, Ch3 p32, Ch3 p34-p35, Ch3 p37, Ch3 p50, Ch3 p53-p54, Ch3 p65-p68, Ch3 p73.||||Overlies the Locker Shale. Overlain by the Muderong Shale.|Sandstones.|
13466|Mungaroo Formation|69689|6|Mentioned|p16|Triassic|Triassic|Northern Carnarvon Basin.||||Overlies Locker Shale. Is overlain by Brigadier Formation.||
13466|Mungaroo Formation|69692|5|Briefly described|p1, 3-5, 9-10, 12, 15, 17, 19|Triassic|Triassic|Seggie et al. (2007). Carnarvon Basin. Several kms thick. Biostratigraphy includes 10 biozones and 18 subzones. Zonation  diagram. Has lateral variability and numerous faults. Regional stratigraphic framework diagram. Six-wells correlation diagram.||||Overlies Locker Shale. Is overlain by Brigadier Formation.|Fluvio-deltaic (channel, floodplain, lacustrine) deposits.|
13466|Mungaroo Formation|70066|5|Briefly described|Dampier: Fig.2;p1-2. Exmouth: Fig.2;p1-4|Norian|Anisian|See also Regional: Fig.6; p4-5, p7-9, p11-13. Northern Carnarvon Basin. Primary gas source for several fields from fluvio-deltaic sediments; hosts the giant accumulations on the Rankin Platform. Claystones provide potential intraformational seals. Fluvial to marginal marine sediments are potential reservoirs (unproven in Beagle Sub-basin).|||Cossigny Member.|Conformably (gradationally) overlies Locker Shale. Is overlain by Brigadier Formation.|A thick fluvio-deltaic succession of sandstone, claystone and minor coal; shoreline sandstone, shallow marine claystone and minor limestone in the upper part.|
13466|Mungaroo Formation|70906|5|Briefly described|p756-758, p760-761, p764, 766-767|Triassic|Triassic|Gorgon Platform. 4953m thick in Clio 1 well. Fault patterns described.||||Overlies Locker Shale. Is overlain by Dingo Claystone.||
13466|Mungaroo Formation|71146|5|Briefly described|p6|Middle Triassic|Middle Triassic|Southern Carnarvon Basin.||||Overlies the Locker Shale.|Sandstone.|
13466|Mungaroo Formation|71342|5|Briefly described|Ch8 p8|Triassic|Triassic|Northern Carnarvon Basin.|||||Shales.|
13466|Mungaroo Formation|72260|4|Described|p1, p3, p4 Fig.3, p5-13, p14-16, p18-21|Norian|Anisian|Occurs within the North Carnarvon Basin; represents a regressive sequence with a maximum thickness of several kilometres(?); basin-scale, low paleo-shelf angle fluvio-deltaic system; reportedly Onslow-Ipswich microfloras; sediment source dominantly from the Ross Delamerian Orogenic belt. Potential monsoonal depositional environment discussed.||||Mungaroo Fm is: underlain by the Locker Shale gradationally; overlain by the Brigadier Formation.|Quartz sandstone, siltstone, shale and coal beds; coarse (conglomeratic) distributary channel sandstones (upward-fining fluvial aggradational cycles with trough crossbedding), organic mudstone and interbedded coal seams.|
13466|Mungaroo Formation|73564|6|Mentioned|p1223, 1225|Triassic|Triassic|Exmouth Plateau, Gascoyne Margin.||||Overlies Locker Shale. Is overlain by Brigadier Formation.||
13494|Munyu Sandstone|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|29807|4|Described|Table 1|||||||||
13494|Munyu Sandstone|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|29817|5|Briefly described|p9|||||||||
13494|Munyu Sandstone|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13494|Munyu Sandstone|31360|4|Described|Table 1|||||||||
13494|Munyu Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13494|Munyu Sandstone|37299|6|Mentioned|Fig.1|||||||||
13494|Munyu Sandstone|45140|2|Defined|p13, p40, p43-46, p48, p56, p58 Fig.43|||See also p60, p75, p83, Appx.p23-24. Blake and Yeates (1977). Named after the Munyu Hills. Birrindudu Basin. Previously mapped as Gardiner Beds (Wells, 1962; Casey and Wells, 1964). 400m thick. The type section is across a strike ridge at 21deg 55'00"S, 128deg 55'00"E in Stansmore sheet area. Forms NE-trending strike ridges. Unconformably overlies Arunta Complex.||Basal Redcliff Pound Group.||Lateral equivalent of Muriel Range and Lewis Range Sandstones, and Vaughan Springs and Heavitree Quartzites. Is overlain by Murraba Formation conformably and Pedestal Beds unconformably.|Medium to thin-bedded, poorly sorted, medium- to very coarse-grained silicified quartz arenite; commonly with scattered pebbles and layers or lenses of grit and quartz-pebble conglomerate. Local limestone lenses and near-base sublithic arenite beds.|
13494|Munyu Sandstone|45155|6|Mentioned|p18|||||||||
13494|Munyu Sandstone|46864|4|Described|p38|||||||||
13494|Munyu Sandstone|62453|6|Mentioned|p16|||Geological Province: Murraba (formerly Birrindudu) Basin.||||||
13494|Munyu Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
13494|Munyu Sandstone|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Quartz sandstone, planar crossbeds, asymmetric ripples; minor conglomerate and siltstone.||||||23-DEC-09
13494|Munyu Sandstone|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Medium to coarse grained sugary massive quartz sandstone; red-brown micaceous silty sandstone.||||||16-AUG-06
13494|Munyu Sandstone|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Quartz sandstone, conglomerate.||||||09-DEC-08
13494|Munyu Sandstone|65074|4|Described|p351 fig 4-37, p353, p356 Tb.4-12|Neoproterozoic|Neoproterozoic|Of SW Birrindudu Basin. 400m thick. Type section is on southeast STANMORE sheet; details given.||Redcliff Pound Group||Overlain by Murraba Formation (conformably). Equivalent to Muriel Range Sandstone and Lewis Range Sandstone.|Quartz arenite, grit, conglomerate, breccia, shale, siltstone, limestone, chert.|
13494|Munyu Sandstone|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group, Murraba Basin. Shown as equivalent age to Vaughan Springs Quartzite, Ngalia Basin. Medium- to coarse-grained sugary massive quartz sandstone; red-brown micaceous silty sandstone||||||02-FEB-10
13494|Munyu Sandstone|65338|6|Mentioned|p59.|||Murraba Basin. Correlated with Vaughan Springs Quartzite.||||||
13494|Munyu Sandstone|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin. See also misspelt Munya Sandstone.||Unit in Redcliff Pound Group.||Is overlain by Murraba Formation.|Quartz sandstone: planar crossbeds, asymmetric ripples, reverse and normal grading; minor conglomerate and siltstone; weakly folded.|19-OCT-11
13494|Munyu Sandstone|68994|4|Described|p1, p8-10, p20, p22, p25, p27|Neoproterozoic|Neoproterozoic|Murraba Basin. Conservative max depositional age of 1155+/-14 Ma, although age of deposition known to be much younger based on correlation with Lewis Range Sandstone. Detrital zircon U-Pb ages listed and Hf analyses detailed. Misspelt as Munya sandstone in Fig.5.|c.1040-820 Ma (Kirkland et al. 2009).|Redcliff Pound Group||Unconformably overlies Lander Rock Formation. Equivalent to Lewis Range Sandstone, Muriel Range Sandstone  and Vaughan Springs Quartzite.|Quartz sandstone, micaceous siltstone, and minor conglomerate.|13-JAN-17
13494|Munyu Sandstone|69031|4|Described|p8|Neoproterozoic|Neoproterozoic|Murraba Basin, west Arunta Orogen. Exposed in the Alec Ross Range, where they are locally folded and faulted. Geochronology by Kirkland et al. (2009).|1155 +/- 14 Ma (maximum depositional age).|Redcliff Pound Group.||Unconformably overlies Lander Rock Formation.|Coarse-grained to pebbly sandstones.|
13494|Munyu Sandstone|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Quartz sandstone with planar crossbeds, asymmetric ripples, and reverse and normal grading; minor conglomerate and siltstone; weakly folded.|
13494|Munyu Sandstone|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.||Redcliff Pound Group.||Is overlain by Murraba Formation.||12-JUL-16
13494|Munyu Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|Murraba Basin. Estimated thickness c.200-400m. Age is poorly constrained; inferred to correlate with Dean and Heavitree Quartzites (Amadeus Basin) and Vaughan Springs Quartzite (Ngalia Basin).||Basal Redcliff Pound Group.||Unconformably overlies Lander Rock Formation and Grimwade Suite. Is overlain conformably by Murraba Formation. Correlates with Denison beds (WA). Equivalent to Muriel Range and Lewis Range Sandstones.|Medium to thickly bedded, fine to coarse quartz sandstone; minor pebble conglomerate; rare thin beds of sublithic siltstone. Local interbedded non-fossiliferous limestone lenses near the top.|12-JUL-16
13494|Munyu Sandstone|69673|5|Briefly described|p187|||Estimated total thickness of 400m.||Redcliff Pound Group||Conformably overlain by Murraba Formation|Quartz sandstone with minor conglomerate and rare sublithic siltstone.|
13494|Munyu Sandstone|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|<1099 Ma.||||Quartz sandstone and conglomerate.|07-NOV-16
13494|Munyu Sandstone|71080|4|Described|p4, 5-p10, 23, p27-p29, 31,36|Tonian|Tonian|Basal unit, southern Murraba Basin. Type section location on Stansmore sheet given. Named after the Munyu Hills in the NT. Outcrops on WEBB, STANSMORE and HIGHLAND ROCKS where it forms strike ridges.Max thickness 400m (Blake et al. 1979). Age inferred from correlations.  Detrital zircon maximum depositional age (1099+/-40 Ma) is similar to that for correlated units, but some of them have other constraints. Previously included in Redcliff Pound Group.The unit closely resembles the Heavitree Formation of the basal Amadeus Basin, with which it has long been correlated. No basal contact with Arunta Orogen basement is exposed in southern Stansmore map sheet area. Appears to be in fault contact with a younger carbonate unit.|Detrital zircon max dep age 1099 +/-40 Ma|||Correlated with Heavitree Formation, Dean Quartzite, Kulail Sandstone of Amadeus Basin; Vaughan Springs Quartzite Ngalia Basin.|Typically a medium-grained, well-sorted quartz sandstone, varying from thin bedded and flaggy, to more commonly thick bedded and blocky. Fine-grained quartz-pebble conglomerate occurs locally.|04-FEB-19
13494|Munyu Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary breccia, shale, sandstone, conglomerate, siltstone|
13494|Munyu Sandstone|71592|5|Briefly described|Appendix A.|||Murraba Basin.|1155+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse- to very coarse-grained sandstone.|
13494|Munyu Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Murraba Basin.|||||Quartz sandstone and conglomerate.|
13494|Munyu Sandstone|73086|6|Mentioned|p9|||Murraba Basin, southern.||||Correlates to Heavitree Formation.||
13494|Munyu Sandstone|73445|5|Briefly described|p3, 6-8, 12-14, 24, 35, 38, 41, 43|Mesoproterozoic|Mesoproterozoic|See also p46 Fig.29, p65-118. Murraba Basin, west Arunta Orogen. Over 400m thick. Whole-rock and regolith chemistries tabulated.|1155 +/- 14 Ma (MDA: Kirkland et al., 2009).|Redcliff Pound Group.||Unconformably overlies Lake McKay Quartzite. Equivalent to Muriel Range and Lewis Range Sandstones.|Silicified quartz arenite, conglomerate, minor limestone.|
13501|Murchison Supergroup|23441|5|Briefly described|p154|||||||||
13501|Murchison Supergroup|23955|6|Mentioned|p1242 Fig.3|||Geological Province: Murchison province, Yilgarn Craton.||||||
13501|Murchison Supergroup|24160|5|Briefly described|p109.||||||Includes Luke Creek and Mount Farmer Groups.|Is overlain by Golconda Formation.||
13501|Murchison Supergroup|42363|5|Briefly described|Fig.1 P312|||||||||
13501|Murchison Supergroup|42533|4|Described|p7|||Archaean||||||
13501|Murchison Supergroup|44149|5|Briefly described|p32, p34-45, p47-49, p51|Archean|Archean|Defined in Watkins and Hickman (in press). Of Murchison Province.|||Includes Luke Creek Group and Mount Farmer Group.|||
13501|Murchison Supergroup|61144|5|Briefly described|p13|Archean|Archean|Includes the Luke Creek and Mount Farmer Groups. Geological Province: Murchison Province.||||||07-NOV-08
13501|Murchison Supergroup|64891|4|Described|p34 Fig. 1, p37 Fig. 2, p48-9 Tb. 1|Archean|Archean|Previously comprised Luke Creek, and Mount Farmer Groups (2 subgroups and 17 formations); the new scheme defines the supergroup as comprising 3 groups - Norie, Polelle and Glen Groups. Age: 2820-2700Ma. Also written as "Murchison Supergroup" (p36).||||||07-FEB-11
13501|Murchison Supergroup|65268|6|Mentioned|p4||||||Includes Luke Creek Group and Mount Farmer Group.|||
13501|Murchison Supergroup|65546|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Includes Polelle Group and various unassigned mafic intrusives -  some deeply weathered. Age given for Meekatharra Formation (?near base of Supergroup?) as 2800-2760 Ma.||||||
13501|Murchison Supergroup|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Youanmi Terrane, Yilgarn Craton. Includes Glen Group, Polelle Group and various unassigned felsic and mafic volcanics  -  some deeply weathered, and metamorphosed.||||||
13501|Murchison Supergroup|65550|5|Briefly described|Map Legend|Archean|Archean|Includes Polelle Group. Of both the Narryer and Youanmi Terranes.||||||18-AUG-10
13501|Murchison Supergroup|66195|5|Briefly described|p599 Fig.2, p611 Fig.9|Neoarchean|Mesoarchean|Includes Golden Grove Group, Norie Group, Polelle Group and Glen Group.||||||
13501|Murchison Supergroup|67116|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Includes Norie, Polelle and Glen Groups.|||
13501|Murchison Supergroup|67129|6|Mentioned|p18 Fig.19, p19 Fig.20, p51, p55|Archean|Archean|Murchison Domain, Youanmi Terrane. Age range from Fig.19. Hosts several layered mafic-ultramafic complexes.|c.2960-c.2724 Ma.||Golden Grove, Mount Gibson, Norie, Polelle, Glen Groups.|||07-SEP-17
13501|Murchison Supergroup|68109|5|Briefly described|p659|||Northern Murchison Domain (Van Kranendonk & Ivanic 2009).|||Includes Norie, Golden Grove, Mount Gibson, Polelle and Glen Groups.|||
13501|Murchison Supergroup|68110|4|Described|p671||Mesoarchean|A Sm-Nd isochron age of 2818 +/- 57 Ma was determined for a unit corresponding to the top of the entire Supergroup. Formerly subdivided into a lower Luke Creek Group and an upper Mount Farmer Group.|< 2818 +/- 57 Ma||Includes Norie, Polelle and Glen Groups.|||05-MAY-16
13501|Murchison Supergroup|68287|5|Briefly described|Map Legend|Mesoarchean|Archean||> 2820 Ma||Includes Norie Group.|||
13501|Murchison Supergroup|68519|5|Briefly described|Map Legend|Neoarchean||Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Includes Norie Group.|||
13501|Murchison Supergroup|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane|||Includes Glen Group,  Polelle Group, Norie Goup and 7 unnamed units.||Metamorphosed iron-formation; Felsic volcanic and volcaniclastic rock; Strongly foliated metabasalt; Mylonitic metabasalt; Mylonitic komatiitic metabasalt; Muscovite-chlorite-quartz mylonite; Mylonitic metakomatiite;|23-OCT-15
13501|Murchison Supergroup|68698|5|Briefly described|p2, p4, p7|Neoarchean|Mesoarchean|Murchison Domain, Yilgarn Craton. Comprises four autochthonous volcano-sedimentary groups.|||Golden Grove, Norie, Polelle and Glen Groups.|||
13501|Murchison Supergroup|69014|6|Mentioned|Map Legend|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane.|||Includes the Polelle Group and the Norie Group.|||
13501|Murchison Supergroup|69267|6|Mentioned|p652-654|||Comprises the supracrustal rocks of the greenstone belts in Murchison Province, Yilgarn Craton. Underwent multiple deformation events.|||Luke Creek, Mount Farmer Groups.|||
13501|Murchison Supergroup|69583|5|Briefly described|p47, p49, p52, p71, p126, p172; Plate 2|Archean|Archean|Murchison Domain, western Youanmi Terrane. Comprises four autochthonous volcano-sedimentary groups. Numerous unnamed units are also mapped separately.|c.2960-2710 Ma.||Weld Range, Minjar, Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|69584|5|Briefly described|p5 Fig.2|Neoarchean|Mesoarchean||||Weld Range Group, Minjar Group, Norie Group, Polelle Group and Glen Group||Andesitic volcanics.|
13501|Murchison Supergroup|69586|5|Briefly described|p22|Neoarchean|Mesoarchean|Murchison Domain.|||Weld Range, Minjar, Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Norie Group|||
13501|Murchison Supergroup|69627|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton|||Polelle Group, Norie Group|||
13501|Murchison Supergroup|69628|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Also includes seven un-named facies, mapped separately.|||Polelle Group, Norie Group||Quartzite, meta-iron formation, metabasalts, mylonite, metamorphosed felsic and intermediate volcaniclastic rocks.|
13501|Murchison Supergroup|70030|5|Briefly described|p189,191-192,208|Neoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.|||Includes Glen, Polelle Norie and Mount Gibson groups.|||
13501|Murchison Supergroup|70139|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|70140|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Also includes 11 un-named facies, of metamorphosed mafic and ultramafic rocks and BIF, that are mapped separately.|2820-2800 Ma.||Norie Group.|||
13501|Murchison Supergroup|70226|5|Briefly described|map legends|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton.|||Glen Group, Polelle Group, Norie Group|||
13501|Murchison Supergroup|70270|6|Mentioned|p520 Fig. 3|||Murchison Province.|||Includes Gossan Hill Group, Thundelarra Group, Minjar Group.|||
13501|Murchison Supergroup|70332|6|Mentioned|p77|Archean|Archean||||Norie Group.|||
13501|Murchison Supergroup|70418|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|70419|6|Mentioned|p1||||||Norie Group.|||
13501|Murchison Supergroup|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2963-2700 Ma.||Norie, Polelle, Glen Groups; Gossan Hill Formation.|||
13501|Murchison Supergroup|70770|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Norie Group.|||
13501|Murchison Supergroup|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, 155568.1.pdf, 155568.1.pdf, 155572.1.pdf, 178142.1.pdf, 183338.1.pdf, 183953.1.pdf, 183975.1.pdf, 185920.1.pdf, 185925.1.pdf, 185928.1.pdf, 185932.1.pdf, 185957.1.pdf, 185959.1.pdf, 185998.1.pdf, 191056.1.pdf, 193972.1.pdf, 193979.1.pdf, 197420.1.pdf, 198209.1.pdf, 198212.1.pdf, 198228.1.pdf, 198293.1.pdf, 198295.1.pdf, 198298.1.pdf, 203702.1.pdf, 203703.1.pdf, 203704.1.pdf, 207686.1.pdf, 211101.1.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, Koonmarra100_2445_stratig.pdf, Madoonga100_2444_stratig.pdf, MountMagnet100_2441_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. Various additional lithologies are provided.|ca 3000 to 2700 Ma (inferred)||Includes the Glen Group, Polelle Group and the Norie Group.|Intruded by the Eelya Suite and the Tuckanarra Suite. Crosscut by the Bald Rock Supersuite.|Basalt, felsic volcanic and volcaniclastic rocks, and clastic and chemical metasedimentary rocks; metamorphosed|
13501|Murchison Supergroup|70826|6|Mentioned|p6 tbl 2, p8|Neoarchean|Mesoarchean|Youanmi Terrane.|||Norie Group, Polelle Group, Glen Group|||22-APR-20
13501|Murchison Supergroup|70830|5|Briefly described|p3, p7-9, p12|Neoarchean|Mesoarchean|Murchison Domain. The Madoonga, Gossan Hill and Mount Gibson formations are newly defined based on contact relationships, geochronology, geochemistry and lithology.|||Includes the Norie Group, Polelle Group, Glen Group, Madoonga Formation, Gossan Hill Formation and the Mount Gibson Formation.|||
13501|Murchison Supergroup|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Norie Group.|||
13501|Murchison Supergroup|71269|4|Described|GEOL_LUT_CSV files + geochron 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, 500k_interpgeop16_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 100k_geologysub_lut.csv.|3000-2700 Ma||Includes Gossan Hill Formation, Madoonga Formation, Glen Group, Norie Group, Poelle Group.|Intruded by Cundimurra Monzogranite. Intruded by Boodanoo Suite.|Amphibolite schist interlayered with metasiliciclastic rock; metamorphosed mafic intrusives and extrusives; felsic volcanics and volcaniclastics; pyroxene spinifex-textured basalt.|
13501|Murchison Supergroup|71271|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.|||Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|71272|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|||Gossan Hill Formation; Norie, Polelle, Glen Groups.|||
13501|Murchison Supergroup|71809|5|Briefly described|map legend|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane|||Includes Norie Group, Polelle Group.|||06-SEP-19
13501|Murchison Supergroup|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane. Subdivided into 6 unnamed units.||Murchison Supergroup|||Amphibolite schist interlayered w metasiliciclastic rock. Mafic intrusive, mafic volcanic or ultramafic rock. Felsic volcanic + volcaniclastic rock; commonly deeply weathered+ kaolinized. Basalt; locally variolitic. All metamorphosed.|
13501|Murchison Supergroup|72389|5|Briefly described|Map Legend|Archean|Archean|Youanmi Terrane, Yilgarn Craton. Gabanintha 1:100k map sheet 2644.|||Includes the Norie and Polelle groups.|||28-AUG-20
13501|Murchison Supergroup|73453|6|Mentioned|p2|||||||||
13501|Murchison Supergroup|73596|6|Mentioned|p1163, 1165, 1172|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane.|||Golden Grove, Norie, Polelle, Glen Groups.|||
13505|Muredong Shale|31899|6|Mentioned|p36|||||||||
13513|Murgurra Shale Member|37460|6|Mentioned|p141|||||||||
13518|Muriel Range Sandstone|29812|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|29817|6|Mentioned|p10|||||||||
13518|Muriel Range Sandstone|31360|6|Mentioned|Table 1|||||||||
13518|Muriel Range Sandstone|31362|4|Described|Table 1|||||||||
13518|Muriel Range Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13518|Muriel Range Sandstone|45140|2|Defined|p13, p22, p40, p43, p46, p48, p75|||See also Appx.p24-25. Hodgson (1976). Named after Muriel Range. Birrindudu Basin. Mapped as Phillipson Beds by Casey and Wells (1964). Forms cuestas and strike ridges. The type section across the Inningarra Range is SW of Mongrel Downs homestead, from 20deg 45'10"S, 129deg 38'45"E to 20deg 47'00"S, 129deg 54'30"E where the unit has its maximum thickness of c.450m. Lithologies described in some detail. Lateral equivalent of Munyu and Lewis Range Sandstones; distinguished by its thin to very thin beds and abundant shale pellets.||Basal Redcliff Pound Group.||Unconformably overlies Pargee Sandstone, Killi Killi and Mount Charles Bed, and The Granites Granite. Is overlain conformably by Murraba Formation, unconformably by Lucas Formation and Pedestal Beds.|Predominantly sublithic arenite and quartz arenite; minor siltstone, shale, arkose, conglomerate and breccia.|
13518|Muriel Range Sandstone|46864|4|Described|p38|||||||||
13518|Muriel Range Sandstone|50315|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Sublithic arente, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age: ~800Ma.||||||02-MAY-07
13518|Muriel Range Sandstone|50374|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group.||||||13-NOV-06
13518|Muriel Range Sandstone|50376|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-APR-06
13518|Muriel Range Sandstone|60676|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Redcliff Pound Group. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-JAN-05
13518|Muriel Range Sandstone|61861|5|Briefly described|p4, p10, 12|||Loosely correlated with Heavitree Quartzite, basal Amadeus Basin. Neoproterozoic?||Unit in Redcliff Pound Group.||Unconformably overlies Dead Bullock Formation, Killi Killi Formation.|Quartz arenite.|
13518|Muriel Range Sandstone|62377|5|Briefly described|p15|||Overlies the Dead Bullock Formation.||||||
13518|Muriel Range Sandstone|62580|6|Mentioned|p10|||||||||07-FEB-11
13518|Muriel Range Sandstone|62628|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose breccia.||||||
13518|Muriel Range Sandstone|65074|4|Described|p351 fig 4-37, p353, p357 Tb. 4-12|Neoproterozoic|Neoproterozoic|Of North/Centre Birrindudu Basin. 450m thick. Type section is in the Inningarra Range; details given.||Redcliff Pound Group||Equivalent to Lewis Range Sandstone and Munyu Sandstone.|Quartz arenite, grit, conglomerate, breccia, shale, siltstone, limestone, chert.|
13518|Muriel Range Sandstone|65194|5|Briefly described|p89 Table 4.3|||Proterozoic sedimentary rocks. Average yield from water bores shown.||||||11-APR-16
13518|Muriel Range Sandstone|65323|5|Briefly described|Map legend, cross sect.|Neoproterozoic|Neoproterozoic|Not present on map; Of the Redcliff Pound Group; arenite, siltstone, shale, conglomerate, arkose, breccia; non-magnetic||||||10-DEC-12
13518|Muriel Range Sandstone|65324|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||
13518|Muriel Range Sandstone|65326|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65327|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65328|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65349|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||
13518|Muriel Range Sandstone|65350|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of Redcliff Pound Group; sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age given as 800 Ma?||||||
13518|Muriel Range Sandstone|65351|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Redcliff Pound Group; sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia. Age given as 800 Ma?||||||02-MAR-10
13518|Muriel Range Sandstone|65352|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65353|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65354|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|65355|5|Briefly described|cross section|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||10-DEC-12
13518|Muriel Range Sandstone|65356|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Of the Redcliff Pound Group||||||12-APR-10
13518|Muriel Range Sandstone|67168|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Redcliff Pound Group.||Unconformably overlies Tanami Group, Inningarra Suite and Pargee Sandstone. Is unconformably overlain by Antrim Plateau Volcanics.|Arenite, siltstone, shale, conglomerate, arkose, breccia.|
13518|Muriel Range Sandstone|68994|6|Mentioned|p20|||Murraba Basin.||||Equivalent to Munyu Sandstone.||13-JAN-17
13518|Muriel Range Sandstone|69440|5|Briefly described|p25:1-2|Cryogenian|Cryogenian|SE Tanami Region; mainly THE GRANITES map area. Maximum thickness of c.450m.||||Correlated with Munyu Sandstone.|Predominantly sublithic arenite and quartz arenite; minor siltstone, shale, arkose, conglomerate and breccia.|12-JUL-16
13518|Muriel Range Sandstone|69673|5|Briefly described|p187|||450m thick.||Redcliff Pound Group|||Sublithic arenite and quartz arenite, minor siltstone, shale, arkose, conglomerate and breccia.|
13518|Muriel Range Sandstone|70852|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Sublithic sandstone, quartz sandstone, minor siltstone, shale, conglomerate, arkosic breccia.|
13518|Muriel Range Sandstone|71080|5|Briefly described|p5-7, p4, p5, p27, 36|||Of Hodgson, 1976, Blake et al. 1979. Up to 450 m thick. Distinguished from its correlatives by its very thin to thin bedding and the abundance of shale pellets. In NT, so not reassessed in this GSWA study. Lies unconformably on Granites-Tanami Orogen and Tanami Basin rocks.||Previously Of Redcliff Pound Group.||Correlated with both the Lewis Range Sandstone and Munyu Sandstone (Blake et al., 1979).|Predominantly sublithic arenite and quartz arenite, but also includes minor siltstone, shale, arkose, conglomerate, and breccia.|04-FEB-19
13518|Muriel Range Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sedimentary breccia, shale, siltstone, arenite, sandstone|
13518|Muriel Range Sandstone|73445|5|Briefly described|p7|||||Redcliff Pound Group.||Equivalent to Munyu and Lewis Range Sandstones.||
13520|Murion Member|42116|5|Briefly described|p71|||||||||
13529|Murraba Formation|22496|6|Mentioned|p10|||||||||
13529|Murraba Formation|23314|5|Briefly described|336|||||||||
13529|Murraba Formation|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|29807|4|Described|Table 1|||||||||
13529|Murraba Formation|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|29813|4|Described|Table 2|||||||||
13529|Murraba Formation|29817|5|Briefly described|p9|||||||||
13529|Murraba Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13529|Murraba Formation|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13529|Murraba Formation|31360|4|Described|Table 1|||||||||
13529|Murraba Formation|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13529|Murraba Formation|45140|2|Defined|p13, p40, p43-45, p47-48, p50-51, p55-56|||See also p58 Fig.43, Appx.p26-27. Blake and Yeates (1977). Named after Murraba Ranges. Birrindudu Basin. Mapped as Gardiner Beds and Phillipson Beds by Casey and Wells (1964). Forms subdued strike ridges and low cuestas. 800m thick; only 350m at the type section at 21deg 36'30"S, 128deg 46'30"E. Folded into gentle curves.||Redcliff Pound Group.||Conformably overlies Munyu and Lewis Range Sandstones. Is overlain by Hazlett Beds, and conformably by Erica Sandstone. Probable correlative of Jawilga Beds and Bitter Springs Formation.|Interbedded chert-granule conglomerate, sublithic arenite, quartz arenite, siltstone, shale, mudstone, pebble conglomerate and dolomite. Beds are mainly thin to laminated.|
13529|Murraba Formation|46864|4|Described|p38|||||||||
13529|Murraba Formation|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Conglomerate, rounded to subangular coarse grained sand to pebbles, quartz and chert clasts, minor arenite.||||||23-DEC-09
13529|Murraba Formation|65074|4|Described|p351 fig 4-37, p353, p356 Tb. 4-12, p362|Neoproterozoic|Neoproterozoic|Of  Birrindudu Basin. 20-800m thick. Type section is at Redcliff Pound.||Redcliff Pound Group||Overlies Munyu and Lewis Range Sandstones conformably. Equivalent to Jawilga beds. Overlain conformably by Erica Sandstone.|Chert-granule conglomerate, arenite, siltstone, shale, mudstone, pebble conglomerate, dolomite.|
13529|Murraba Formation|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Unit in Redcliff Pound Group.||Overlies Munyu Sandstone. Is overlain by Erica Sandstone.|Conglomerate: rounded to subangular coarse-grained sand to pebbles, quartz and chert clasts; minor arenite.|19-OCT-11
13529|Murraba Formation|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Conglomerate with rounded to subangular coarse-grained sand to pebbles, quartz and chert clasts, minor arenite.|
13529|Murraba Formation|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.||Redcliff Pound Group.||Overlies Munyu Sandstone. Is overlain by Erica Sandstone.||12-JUL-16
13529|Murraba Formation|69440|4|Described|p25:1-3|Cryogenian|Cryogenian|Murraba Basin. Most extensive exposures are in WA; some outcrops occur in the Sydney Margaret Range. Up to 800m thick. Interpreted to have been deposited in fluvial to less-common shallow-marine environments and at times was emergent.||Redcliff Pound Group.||Conformably overlies Munyu and Lewis Range Sandstones. Is overlain conformably by Erica Sandstone. Correlates with Jawilga beds (WA).|Conglomerate, sublithic and quartz sandstone; rare mudstone and dolostone.|12-JUL-16
13529|Murraba Formation|69673|5|Briefly described|p187|||800m thick (in WA).||Redcliff Pound Group||Conformably overlies Munyu Sandstone, conformably overlain by Erica Sandstone|Conglomerate and sublithic sandstone, quartz sandstone, with rare mudstone and dolostone.|
13529|Murraba Formation|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.|||Chert-clast granule and pebble conglomerate, sandstone, siltstone and mudstone; minor limestone; thin-bedded (section only).|
13529|Murraba Formation|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Overlies Lewis Range Sandstone. Is overlain by Erica Sandstone.|Chert-clast granule and pebble conglomerate, sandstone, siltstone and mudstone; minor limestone; thin-bedded.|
13529|Murraba Formation|71080|4|Described|p11-p18, 21, 27, 28, 29, 32,36-37|Ediacaran|Ediacaran|Murraba Basin. Named for the Murraba Ranges on STANSMORE. 350 m thick in type section. Definition needs revision. Cenozoic cover obscures previously inferred relationships in Stansmore map sheet area. Picking boundary with overlying Erica Sandstone is problematic. Thickness estimated at 220m at western end of Phillipson Range. Includes Arumberia and tubular body fossils. See also p4, 5,||Redcliff Pound Group||Basal unconformity inferred. Conformably overlain by Erica Formation.|Interbedded chert-granule conglomerate, sublithic arenite, quartz arenite, siltstone, shale, pebble conglomerate and dolomite.|04-FEB-19
13529|Murraba Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, shale, conglomerate|
13529|Murraba Formation|73445|5|Briefly described|p7-8, 10|||The boundary with Erica Sandstone is time-transgressive.||Redcliff Pound Group.||Overlies Lewis Range Formation. Is overlain by Erica Sandstone.|Siliciclastic sedimentary rocks.|
13534|Murramunda Dolerite|41768|5|Briefly described|p55|||||||||
13534|Murramunda Dolerite|42704|5|Briefly described|Plate 1|Proterozoic||Fine-grained to weakly porphyritic dolerite.||||||07-AUG-08
13534|Murramunda Dolerite|44151|6|Mentioned|p160 Fig.2-146|||Appears as Murramunda dolerite.||||||
13534|Murramunda Dolerite|64384|5|Briefly described|p92|||Intrudes the Sylvania Inlier.||||||07-FEB-11
13546|Murray Range Gabbro|30389|6|Mentioned|p13|||||||||
13546|Murray Range Gabbro|61341|5|Briefly described|Map legend|||Presented as the compound name Murray Range Pyroxenite/Peridotite/Gabbro Intrusion.||||||21-SEP-05
13546|Murray Range Gabbro|68996|5|Briefly described|p5, p7, p36, p43, p57|Mesoproterozoic|Mesoproterozoic|G2 group. Shown as Murray Range Gabbro p7, 36,43 . See also map p50.||Giles Suite||Fault bounded.||
13596|Musgrave Complex|22506|6|Mentioned|p129|||||||||
13596|Musgrave Complex|22635|6|Mentioned|p492||Mesoproterozoic|||||||
13596|Musgrave Complex|22806|5|Briefly described|p484||Precambrian|||||||
13596|Musgrave Complex|22824|6|Mentioned|Fig 1 on p530|||||||||
13596|Musgrave Complex|22826|6|Mentioned|Fig 1 on p564|||||||||
13596|Musgrave Complex|23205|6|Mentioned|p302|Proterozoic|Proterozoic|||||||
13596|Musgrave Complex|23463|6|Mentioned|p240|||||||||
13596|Musgrave Complex|23571|5|Briefly described|p4 Fig. 2, p7|||Geological Province: Officer Basin. Overlain by Townsend Quartzite (unconformable)||||||13-NOV-06
13596|Musgrave Complex|23590|6|Mentioned|p4|||||||||
13596|Musgrave Complex|23745|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Also called Wingelina complex. Age: c.1550-1200 Ma.||||||
13596|Musgrave Complex|23758|6|Mentioned|p5|||||||||
13596|Musgrave Complex|23760|6|Mentioned|p5|||||||||
13596|Musgrave Complex|24115|6|Mentioned|p28|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|24390|6|Mentioned|p9|||||||||
13596|Musgrave Complex|24410|6|Mentioned|p36, p37|||Name used in structural context.||||||
13596|Musgrave Complex|24535|6|Mentioned|p16, p19 Fig.15|Mesoproterozoic|Mesoproterozoic|Text uses this name as a geological province. Fig 15 shows includes bimodal magmatism 1090 - 1049 Ma.||||||
13596|Musgrave Complex|38066|5|Briefly described|p50|||||||||
13596|Musgrave Complex|41190|6|Mentioned|p264|||||||||
13596|Musgrave Complex|41270|6|Mentioned|p267|||||||||
13596|Musgrave Complex|41594|5|Briefly described|p72|||||||||
13596|Musgrave Complex|41717|6|Mentioned|p248|||||||||
13596|Musgrave Complex|41852|5|Briefly described|p208|||||||||
13596|Musgrave Complex|42049|6|Mentioned|Fig.1 P216|||||||||
13596|Musgrave Complex|42730|4|Described|p16|||||||||
13596|Musgrave Complex|43442|6|Mentioned|Fig.5,p16|||Probably used as a geological province.||||||
13596|Musgrave Complex|49895|6|Mentioned|p5|||||||||
13596|Musgrave Complex|50008|6|Mentioned|p47 Fig.4|||||||||
13596|Musgrave Complex|50085|6|Mentioned|p9|||Geological Province: Officer Basin.||||||
13596|Musgrave Complex|50127|6|Mentioned|p48 Fig. 2|||Structural term.||||||
13596|Musgrave Complex|50205|6|Mentioned|p60|||Includes the Tollu Volcanics.||||||
13596|Musgrave Complex|50222|6|Mentioned|p334 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1.06Ga.||||||
13596|Musgrave Complex|50228|5|Briefly described|p477|Mesoproterozoic|Mesoproterozoic|Geological Province: West Australian Craton.||||||
13596|Musgrave Complex|50544|6|Mentioned|p55, p60|||Intended as a structural term in this context.||||||
13596|Musgrave Complex|50621|6|Mentioned|p165 Fig.6, p167|||Geological Province Paterson Orogen.||||||
13596|Musgrave Complex|60470|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Includes zircon-bearing rocks of ~1070 Ma. Possible source material for Throssell Range and Lamil Group rocks.||||||
13596|Musgrave Complex|61023|6|Mentioned|p13|||||||||
13596|Musgrave Complex|61064|5|Briefly described|p5, p12|Neoproterozoic|Mesoproterozoic|See also pages 38 and 49.||||||
13596|Musgrave Complex|61272|5|Briefly described|p123 Fig.4|||Unconformably overlain by the Townsend Quartzite.||||||
13596|Musgrave Complex|61306|6|Mentioned|p11|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
13596|Musgrave Complex|61564|6|Mentioned|p589 Fig. 1|||Structural term in this context.||||||
13596|Musgrave Complex|61732|6|Mentioned|p36, p56, p84|||Structural term in this context. See also p90.||||||07-FEB-11
13596|Musgrave Complex|61733|5|Briefly described|p55|||Discussion of crustal material required for Nd isotopic signature.|||||Felsic gneisses.|
13596|Musgrave Complex|62453|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|62986|6|Mentioned|p18|||||||||
13596|Musgrave Complex|62987|6|Mentioned|p30|||||||||
13596|Musgrave Complex|63465|6|Mentioned|p553 Fig. 2|||Includes granulites.||||||
13596|Musgrave Complex|63869|6|Mentioned|p3 Fig.1|||||||||
13596|Musgrave Complex|64283|6|Mentioned|p55|||||||||07-FEB-11
13596|Musgrave Complex|64325|6|Mentioned|p80, p84, p85|Mesoproterozoic|Mesoproterozoic|||||||
13596|Musgrave Complex|64577|6|Mentioned|p605|||||||||
13596|Musgrave Complex|64635|6|Mentioned|p2 Fig.1|||||||||
13596|Musgrave Complex|64777|6|Mentioned|p1 Fig.1, p3, p7-8|||||||||
13596|Musgrave Complex|64793|6|Mentioned|p282 Fig.1|||||||||
13596|Musgrave Complex|64943|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Of central Australia (Williams and Myers 1990). Considered part of the Paterson Orogen.||||||
13596|Musgrave Complex|65363|6|Mentioned|p4.|||||||||
13596|Musgrave Complex|65410|6|Mentioned|p73 Fig.2.|Proterozoic|Proterozoic|Officer and Amadeus Basins.||||||
13596|Musgrave Complex|65416|5|Briefly described|pp135-137, p145.|Mesoproterozoic|Paleoproterozoic|Western Officer Basin. Metasedimentary and meta-igneous rocks, overlain by Mission and Cassidy Groups. Post-Cambrian movement saw this unit stepped further to the south than the Rudall Complex.||||||
13596|Musgrave Complex|65454|6|Mentioned|p12|||||||||
13596|Musgrave Complex|65487|6|Mentioned|p9|||Potentially contiguous with the Albany-Fraser Orogen to the SW.||||||
13596|Musgrave Complex|65826|6|Mentioned|p5. |Proterozoic|Proterozoic|Paterson Orogen rocks outcrop in this part of central Australia. Name used in 'geological province' sense.||||||23-MAY-16
13596|Musgrave Complex|65833|4|Described|p1-18|Neoproterozoic|Mesoproterozoic|Includes Wirku Metamorphics.||||||
13596|Musgrave Complex|66256|6|Mentioned|p2|||Of Myers et al. (1996). Term now replaced by Musgrave Province.||||||
13596|Musgrave Complex|66427|6|Mentioned|p40 Fig.1|||Mafic magmatism c.1.06 Ga.||||||
13596|Musgrave Complex|67581|6|Mentioned|p44 Fig.8|||||||||
13596|Musgrave Complex|70125|6|Mentioned|p403, p408|||Central Australia.||||||
13596|Musgrave Complex|70634|6|Mentioned|174558.1.pdf|||Used interchangeably as a geological province.|||Includes Pitjantjatjara Supersuite, Wirku Metamorphics|||
13596|Musgrave Complex|72476|6|Mentioned|p36|||Detrital zircon ages suggest the Musgrave Block was exhumed 590 Ma and 420 Ma.||||||
13681|Nadarra Formation|23310|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
13681|Nadarra Formation|23311|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
13681|Nadarra Formation|23312|5|Briefly described|map legend|Pleistocene|Pliocene|||||||
13681|Nadarra Formation|23403|6|Mentioned|p5|||||||||
13681|Nadarra Formation|23726|5|Briefly described|p42|Cenozoic|Cenozoic|||||||19-NOV-08
13681|Nadarra Formation|23815|6|Mentioned|p305|Pleistocene|Pleistocene|Geological Province: Carnarvon Basin.||||||18-APR-05
13681|Nadarra Formation|23978|5|Briefly described|Map Legend|||||||||
13681|Nadarra Formation|34231|6|Mentioned|p66|||?equivalent.||||||
13681|Nadarra Formation|36890|6|Mentioned|p305|||||||||
13681|Nadarra Formation|38493|4|Described|p36|||||||||
13681|Nadarra Formation|39370|5|Briefly described|p37|||||||||
13681|Nadarra Formation|41271|4|Described|p198|||Mention P200||||||
13681|Nadarra Formation|42116|6|Mentioned|p31|||||||||
13681|Nadarra Formation|43255|5|Briefly described|map legend|Pleistocene|Miocene|Age ?Miocene to Pleistocene.||||||
13681|Nadarra Formation|43256|5|Briefly described|19|Pleistocene|Pliocene|||||||
13681|Nadarra Formation|44344|14|Not recorded|p.19, opp.4, map|||(G50-1).||||||
13681|Nadarra Formation|44345|14|Not recorded|map legend||Pleistocene|Pleistocene.||||||
13681|Nadarra Formation|44532|4|Described|p.10, map|||(G50-5).||||||
13681|Nadarra Formation|44533|5|Briefly described|map legend||Pleistocene|Pleistocene.||||||
13681|Nadarra Formation|45015|5|Briefly described|map legend|Quaternary|Quaternary|Geological Province: Carnarvon Basin.||||||31-MAY-06
13681|Nadarra Formation|61155|5|Briefly described|p15|Late Pliocene|Early Pliocene|Partly overlain by Exmouth Sandstone. Age: 4.5-2.5Ma.  Geological Province: Carnarvon Basin /onshore.||||||
13681|Nadarra Formation|61958|5|Briefly described|Map sheet 1|Quaternary||||||||
13681|Nadarra Formation|63469|5|Briefly described|map legend|Neogene|Neogene|Consists of silty micritic limestone, in part chalcedonic, light grey, laustrine.||||||24-SEP-07
13681|Nadarra Formation|65829|6|Mentioned|p31.|||Carnarvon Basin. Resembles Oakover Formation.||||||
13681|Nadarra Formation|66579|5|Briefly described|Map legend|Neogene|Neogene|Southern Carnarvon Basin.|||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine.|
13681|Nadarra Formation|67373|5|Briefly described|Map legend.|Pleistocene|Pliocene|Southern Carnarvon Basin.|||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine.|
13681|Nadarra Formation|69011|5|Briefly described|Map Legend|Quaternary|Neogene||||||Comprises silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine; may extend into Pleistocene.|
13681|Nadarra Formation|69028|5|Briefly described|Map Legend|Pleistocene|Pleistocene||||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine.|17-SEP-15
13681|Nadarra Formation|69166|5|Briefly described|geologyp_lut.csv|Pleistocene|Pliocene||||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine|
13681|Nadarra Formation|70795|4|Described|100k_geologyp_lut.csv|Pliocene|Pliocene|Also 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|5-2.5 Ma||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine.|
13681|Nadarra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone, micrite|
13681|Nadarra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Pliocene|Pliocene|Valley-fill deposits, Southern Carnarvon Basin. May extend into Pleistocene.|||||Silty micritic limestone; includes minor calcrete; muddy, commonly silicified; lacustrine; may extend into Pleistocene.|
13690|Nakina Formation|14227|5|Briefly described|Enclos. 2|Early Cretaceous|Early Cretaceous|Presented as Nakina FM.||||||07-FEB-11
13690|Nakina Formation|23880|5|Briefly described|p41|Early Cretaceous|Early Cretaceous|||||||
13690|Nakina Formation|24410|6|Mentioned|p108|Tertiary|Tertiary|Sandy alluvial deposits. In the Collie area. Geological Province: Yilgarn Craton. See also p113 Fig. 62.||||||28-JUL-09
13690|Nakina Formation|29693|6|Mentioned|p35|||||||||
13690|Nakina Formation|30268|6|Mentioned|p42|||||||||
13690|Nakina Formation|31911|5|Briefly described|p96|||||||||
13690|Nakina Formation|33801|6|Mentioned|p51|||||||||
13690|Nakina Formation|36265|5|Briefly described|p136, Fig. 3.28|Tertiary|Tertiary|Unconformably overlies Collie Coal Measures. Max. thickness: 30m. Geological province: Shotts Sub-basin. Probably Late Tertiary age.||||||28-JUL-09
13690|Nakina Formation|36890|3|Fully described|p424|||Formerly Collie Lake Beds||||||
13690|Nakina Formation|37105|4|Described|p273|||Formerly Lake Beds||||||
13690|Nakina Formation|37133|6|Mentioned|p377|||||||||
13690|Nakina Formation|37341|4|Described|p231|||||||||
13690|Nakina Formation|37350|6|Mentioned|Fig.1|||||||||
13690|Nakina Formation|37577|6|Mentioned|p63|||||||||
13690|Nakina Formation|37633|6|Mentioned|p69|||||||||
13690|Nakina Formation|38437|6|Mentioned|p434|||||||||
13690|Nakina Formation|38936|4|Described|p324|||||||||
13690|Nakina Formation|40359|5|Briefly described|p25|||||||||
13690|Nakina Formation|40360|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13690|Nakina Formation|41780|5|Briefly described|p2|||Previously known as "Lake Beds"||||||
13690|Nakina Formation|41785|5|Briefly described|p85|||||||||
13690|Nakina Formation|41984|5|Briefly described|Fig.2 P4|||||||||
13690|Nakina Formation|42309|4|Described|p238|Early Cretaceous||||||||
13690|Nakina Formation|42431|5|Briefly described|p237|||Collie & Boyup Basins||||||
13690|Nakina Formation|42711|2|Defined|p5 Fig. 4, p28, Plates 4, 5|Cretaceous|Cretaceous|Formerly "Lake Collie Beds" of Maitland (1919). Unconformably overlies Muja C.M (Collie Group). Overlies Collie Group with erosional contact. Weakly lithified claystone, conglomerate and sandstone in upward-fining cycle.||||||11-AUG-08
13690|Nakina Formation|43068|5|Briefly described|Table 2,p138|||||||||
13690|Nakina Formation|43212|6|Mentioned|p6||Cretaceous|||||||
13690|Nakina Formation|61155|5|Briefly described|p17|Late Eocene|Middle Eocene|Geological region: Darling Range.||||||
13690|Nakina Formation|67861|4|Described|p530, 527 tab 4-22, p528 fig 4-172|Cretaceous|Cretaceous|Collie Basin. Contains Cretaceous microflora. Maximum thickness 20m. Stratigraphic integrity in doubt. May require revision.||||Unconformably overlies Collie Coal Measures.|Poorly lithified cross-bedded sands, silty clays and clays with lateritic hardcap.|
13690|Nakina Formation|67862|6|Mentioned|p534|Cretaceous|Cretaceous|Of Collie Basin. Up to 20m of micaceous siltstone overlying Collie Coal Measures in Wilga Basin may be Cretaceous Nakina Formation.||||||
13690|Nakina Formation|70097|5|Briefly described|p19 Fig.3|Aptian|Aptian|Southern Perth Basin. Collie Sub-basin.||||Overlies Muja Coal Measures.|Sandstone.|12-SEP-17
13690|Nakina Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||alluvial sediment|
13698|Nalbia Sandstone|13615|6|Mentioned|p17, 62|||Peedamullah Shelf. Previously recognised in Ruby 1 (Mills, 1997), but this interval now assigned to Abdul Sandstone.||||||09-FEB-19
13698|Nalbia Sandstone|14228|6|Mentioned|p8|Kungurian|Kungurian|||Byro Group||||
13698|Nalbia Sandstone|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
13698|Nalbia Sandstone|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
13698|Nalbia Sandstone|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
13698|Nalbia Sandstone|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
13698|Nalbia Sandstone|23726|5|Briefly described|p7 Fig 2b|Early Permian|Early Permian|Of Byro Group. Overlying unit Baker Formation. Underlying unit Wandagee Formation. Geological Province: Carnarvon Basin.||||||
13698|Nalbia Sandstone|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
13698|Nalbia Sandstone|34277|6|Mentioned|Table 1|||Permian||||||
13698|Nalbia Sandstone|37294|6|Mentioned|p100|||||||||
13698|Nalbia Sandstone|37295|6|Mentioned|p51|||Proposed usage.||||||
13698|Nalbia Sandstone|37304|6|Mentioned|p55|||||||||
13698|Nalbia Sandstone|39223|6|Mentioned|p242|||||||||
13698|Nalbia Sandstone|39316|6|Mentioned|Fig.2|||||||||
13698|Nalbia Sandstone|39974|6|Mentioned|p113|||||||||
13698|Nalbia Sandstone|40617|6|Mentioned|Fig.1|||||||||
13698|Nalbia Sandstone|41071|6|Mentioned|p25|||||||||
13698|Nalbia Sandstone|41271|3|Fully described|p98|||||||||
13698|Nalbia Sandstone|41438|6|Mentioned|Fig.11|||||||||
13698|Nalbia Sandstone|41632|6|Mentioned|p1|||||||||
13698|Nalbia Sandstone|42116|5|Briefly described|p41|||||||||
13698|Nalbia Sandstone|42392|6|Mentioned|p118|||Byro Group||||||
13698|Nalbia Sandstone|42598|6|Mentioned|Fig 36(P 38)|||||||||
13698|Nalbia Sandstone|42654|6|Mentioned|p6|||||||||
13698|Nalbia Sandstone|42994|6|Mentioned|p37|||||||||
13698|Nalbia Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
13698|Nalbia Sandstone|44657|14|Not recorded|p.10|||F/49-16-Minilya.||||||
13698|Nalbia Sandstone|45016|14|Not recorded|p.173|||Ref. to Teichert 1950.||||||
13698|Nalbia Sandstone|49644|5|Briefly described|Table|||||||||
13698|Nalbia Sandstone|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of Byro Group. Overlies Wandagee Formation. Overlain by Baker Formation. Geological Province: Southern Carnarvon Basin.||||||
13698|Nalbia Sandstone|64580|5|Briefly described|map legend|||Of Upper Byro Group. Black shale to mudstone overlying fine-grained sandstone and shale.||||||15-DEC-08
13698|Nalbia Sandstone|64974|6|Mentioned|p146, p147 Fig. 5|Kungurian|Kungurian|Geological Province: Carnarvon Basin.||||||24-JUN-09
13698|Nalbia Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes brown meduim-grained sandstone, occasional bioturbation.|23-DEC-22
13698|Nalbia Sandstone|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 2.99 W/mK. See also p47, p54, app 2 p5.||Byro Group||Overlies Wandagee Formation, overlain by Baker Formation|Interbedded, bioturbated siltstone and medium grained sandstone with planar cross bedding.|
13698|Nalbia Sandstone|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.|||Comprises fine-grained sandstone; minor siltstone.|
13698|Nalbia Sandstone|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
13698|Nalbia Sandstone|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Wandagee and Baker Formations.||Byro Group.|||Intercalated siltstone, shale and sandstone.|
13698|Nalbia Sandstone|70795|5|Briefly described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group|||Fine-grained sandstone; minor siltstone.|
13698|Nalbia Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke|
13698|Nalbia Sandstone|72910|4|Described|p10, p,18, p23, p30, p38, p41.|Kungurian|Kungurian|Thickness 40-120m. Nalbia Type section located 4km north of Wandagee Hill, 23d48m10sS; 114d25m10sE. m. Said to be Artinskian age p38.||Byro Group||Overlies Quinnanie Shale. Conformably overlies Wandagee Formation and conformably underlies Baker Formation.|Fine sandstone, minor siltstone, abundant Zoophycos.|
13699|Nallanaring Volcanic Member|23570|4|Described|p237 App. 1|||Abbreviated to Nallanaring Member by authors.  Overlain by Roy Hill Shale; underlain by the Warrie Member.   Max. thickness: 76m.   Geological Province: Pilbara Craton||||||
13699|Nallanaring Volcanic Member|24353|4|Described|p6|Archean|Archean|Parent: Jeerinah Formation. Geological Province: Pilbara Craton||||||07-NOV-08
13699|Nallanaring Volcanic Member|30490|6|Mentioned|p112|||||||||
13699|Nallanaring Volcanic Member|35260|5|Briefly described|Table 1|||||||||
13699|Nallanaring Volcanic Member|36882|6|Mentioned|p124|||||||||
13699|Nallanaring Volcanic Member|37460|3|Fully described|Table 3.I|||||||||
13699|Nallanaring Volcanic Member|39030|5|Briefly described|p3|||||||||
13699|Nallanaring Volcanic Member|39426|6|Mentioned|p11|||||||||
13699|Nallanaring Volcanic Member|39697|6|Mentioned|p124|||||||||
13699|Nallanaring Volcanic Member|41687|5|Briefly described|p95|||||||||
13699|Nallanaring Volcanic Member|42785|5|Briefly described|p270|||same as Nallanaring Ignimbrite.||||||
13699|Nallanaring Volcanic Member|44152|5|Briefly described|p174|||||Jeerinah Formation|||Includes felsic, as well as basaltic, lavas and pyroclastic rocks.|
13699|Nallanaring Volcanic Member|44477|2|Defined|p.29, p.9, Table 1||Proterozoic|SF/50-6.||||||
13699|Nallanaring Volcanic Member|44478|14|Not recorded|map legend||Proterozoic|||||||
13699|Nallanaring Volcanic Member|46319|6|Mentioned|p14|||||||||
13699|Nallanaring Volcanic Member|67229|6|Mentioned|p3 Fig.2|||Williams (1968).||Jeerinah Formation.||||
13699|Nallanaring Volcanic Member|69299|5|Briefly described|p7|||Of Kriewaldt and Ryan (1967)|2684 +/- 6 Ma (Arndt et al. 1991).|Of Jeerinah Formation.|||Felsic volcanics.|01-JUL-14
13699|Nallanaring Volcanic Member|72569|6|Mentioned|p2|||Of the Hamersley Basin.||Jeerinah Formation||||
13709|Namban Granite|40348|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
13709|Namban Granite|40349|5|Briefly described|p11|||||||||
13709|Namban Granite|64769|5|Briefly described|p112, p113|Archean|Archean|Coarse-grained, pink and green, mainly megacrystic granites ranging in composition from monzogranite to quartz monzonite, and quartz syenite at different sites.||||||
13709|Namban Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
13720|Nammuldi Member|23126|4|Described|p382|||||||||
13720|Nammuldi Member|42112|5|Briefly described|p17|||Reserved as Nammuldi.||||||08-APR-09
13720|Nammuldi Member|42190|6|Mentioned|Fig.3 P273|||||||||
13720|Nammuldi Member|42471|5|Briefly described|p7|||of Marra Mamba Iron Formation.||||||
13720|Nammuldi Member|42744|4|Described|p4|||Of Marra Mamba Iron Formation.||||||08-APR-09
13720|Nammuldi Member|43063|3|Fully described|p56|||Of Marra Mamba Iron Formation.||||||08-APR-09
13720|Nammuldi Member|43119|5|Briefly described|p9|||Of Marra Mamba Iron Formation.||||||08-APR-09
13720|Nammuldi Member|43210|5|Briefly described|Table1 p3.|||of Marra Mamba Iron Formation||||||
13720|Nammuldi Member|43290|5|Briefly described|p6||Archean|of Marra Mamba Iron Formation.||||||07-NOV-08
13720|Nammuldi Member|44152|5|Briefly described|p179 Fig.2-155|||||Marra Mamba Iron Formation||Is overlain by Mount MacLeod Member.|BIF.|
13720|Nammuldi Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Marra Mamba Iron Formation.||||||23-JUN-09
13720|Nammuldi Member|60706|5|Briefly described|p623 Fig.2|||Of the Marra Mamba Iron Formation (Hamersley Group). Geological Province: Hamersley Basin. See also Appendix 1 p644.H61||||||
13720|Nammuldi Member|62129|3|Fully described|p9|Archaean|Archaean|Of Marra Mamba Iron Formation. Overlain by MacLeod Member. Thickness: 100m. Geological Province: Hamersley Basin. Alternating yellow to yellow-brown chert and brown to black iron-formation mesobands.||||||07-FEB-11
13720|Nammuldi Member|63153|6|Mentioned|p1359-1368, p1370-1371, p1373, p1375. |||Shows numerous sedimentary structures characteristic of current deposition. Magnetite-silicate BIF is abundant.||Basal unit in Marra Mamba Iron Formation.||Overlies Jeerinah Formation. Is overlain by MacLeod Member.|Includes high-grade hematite ore together with low-grade limonitic ore that becomes high-grade after calcining.|
13720|Nammuldi Member|64384|5|Briefly described|p35 Tb. 6|||Basal unit of Marra Mamba Iron Formation (Hamersley Group). Geological province: Hamersley Basin. Yellow-weathering chert, cherty BIF, some shale bands.||||||07-FEB-11
13720|Nammuldi Member|65683|5|Briefly described|p799, p800, p801 Fig2, p804-5|||Lowest unit of the Marra Mamba Iron Formation. Underlies MacLeod Member; conformably overlies Roy Hill Shale of the Jeerinah Formation. Iron formation.||||||08-MAR-12
13720|Nammuldi Member|67056|5|Briefly described|p419 Fig.2, p422 Fig.3(c), p425. |||Hosts the Cloud Break and Christmas Creek iron ore deposits; dominantly martite-goethite supergene enrichment. Tonnage per strike km c.25 Mt.||Basal unit in Marra Mamba Iron Formation.||Is overlain by MacLeod Member.||
13720|Nammuldi Member|67130|5|Briefly described|p3 fig 2|||||Marra Mamba Iron Formation||Overlies Jeerinah Formation, overlain by MacLeod Member|Banded iron formation|
13720|Nammuldi Member|67201|6|Mentioned|p34 Fig.18|||||Marra Mamba Iron Formation||||24-NOV-16
13720|Nammuldi Member|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean|Approximately 80 m thick.|c. 2597 Ma|Of the Marra Mamba iron formation.|||Cherty banded iron formation.|
13720|Nammuldi Member|67827|5|Briefly described|p415|||Contains supergene ore. Microstructure of iron ores discussed.||Of the Marra Mamba Iron Formation.||||
13720|Nammuldi Member|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin.||Of Marra Mamba Iron Formation.||Overlies Jeerinah Formation. Overlain by MacLeod Member.|Banded iron formation.|
13720|Nammuldi Member|68280|6|Mentioned|p5|||||Marra Mamba Iron Formation|||Banded iron formation.|
13720|Nammuldi Member|69538|6|Mentioned|p516, p517 Fig.3, p583-585|||||Unit in Marra Mamba Iron Formation.||||
13720|Nammuldi Member|71808|4|Described|vi, p2, p11-p13, p16, p18-p19|||Hamersley Province. Up to 90m thick. In outcrop this unit is typically well silicified and dominated by poorly bnedded, yellow chert and biffy chert, typically with broad pinch and swell structures or undulating bedding. Distinguishing characteristics are described. See also p45, p53, p71, p73, p85, p117, p127, p129, p153, p166, p168, p224-p225, p237.||Marra Mamba Iron Formation|||Carbonates overlain by silicified cherty carbonate and cherty banded iron formation with minor interbedded tuffaceous shales.|
13720|Nammuldi Member|72493|5|Briefly described|p30|||Hamersley Basin.||Marra Mamba Iron Formation.||Overlies Jeerinah Formation. Is overlain by McLeod Member.|BIF.|
13720|Nammuldi Member|73022|6|Mentioned|p3 Fig.2|||||Marra Mamba Iron Formation||Overlies the Jeerinah Formation, underlies the MacLeod Member.|Fe-chert and minor shale.|
13720|Nammuldi Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
13720|Nammuldi Member|73538|6|Mentioned|p4|||[Misspelt as Nammudi Member, p4].||Marra Mamba Iron Formation||Underlain by the Jeerinah formation of the Fortescue Group. Overlain by MacLeod Member.|Iron formation.|
13755|Nanarup Limestone Member|23331|6|Mentioned|1088|||||||||
13755|Nanarup Limestone Member|23533|5|Briefly described|p561|Eocene|Eocene|Of Werrilup Formation. Geological Province: Bremer Basin.||||||
13755|Nanarup Limestone Member|23768|6|Mentioned|p59|Aldingan|Aldingan|Of Werrillup Formation.||||||
13755|Nanarup Limestone Member|23817|5|Briefly described|p430|Tertiary|Tertiary|Formerly known as the "Nannarup Limestone".  Geological Province: Bremer Basin.  Of the Werillup Formation.  Max. Thickness 4.6m.  Fossiliferous.||||||
13755|Nanarup Limestone Member|24094|5|Briefly described|p270|Middle Eocene|Middle Eocene|Of Werillup Formation. See also Nanarup Limestone. Geological Province: Bremer Basin||||||16-MAR-05
13755|Nanarup Limestone Member|24397|6|Mentioned|p237|||||||||
13755|Nanarup Limestone Member|32311|4|Described|p12|||Fossiliferous||||||
13755|Nanarup Limestone Member|32743|6|Mentioned|p179|||See also P183. U.Eocene||||||
13755|Nanarup Limestone Member|32750|6|Mentioned|p306|||Refers faunas Quilty (1969,1970)||||||
13755|Nanarup Limestone Member|34432|6|Mentioned|p41|||Middle Eocene. See also PP42,56||||||
13755|Nanarup Limestone Member|36200|6|Mentioned|p11|||||||||
13755|Nanarup Limestone Member|36890|4|Described|p430|||Formerly Nanarup Limestone""||||||
13755|Nanarup Limestone Member|37596|5|Briefly described|p79|||||||||
13755|Nanarup Limestone Member|38214|6|Mentioned|p246|||||||||
13755|Nanarup Limestone Member|39795|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13755|Nanarup Limestone Member|41626|6|Mentioned|p50|||||||||
13755|Nanarup Limestone Member|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|||||||
13755|Nanarup Limestone Member|44146|5|Briefly described|p562, Fig.4-200, p563 Table 4-28|Eocene|Eocene|Bremer Basin. Algae, forams, bryzoans, echinoids, brachiopods, molluscs indicate late Middle to late Eocene age||Of Werillup Formation|||Friable limestone.|
13755|Nanarup Limestone Member|71789|2|Defined|p100||Late Eocene|Member Werillup Formation. Type section in Nanarup lime quarry. 15 ft thick. Included in Werillup Formaion on basis of fossils. No contacts exposed.||||||28-MAY-19
13780|Nangetty Formation|12758|5|Briefly described|p8 Fig. 9|Permian|Permian|Geological Province: Northern Perth Basin.||||||
13780|Nangetty Formation|14227|5|Briefly described|p7, p9|Early Permian|Early Carboniferous|Geol. Prov: Bunbury Trough, Perth Basin. Glacio-marine sediments. See also Enclosure 2 where presented as Nangetty only.||||||07-FEB-11
13780|Nangetty Formation|22814|5|Briefly described|fig2|Early Permian||||||||
13780|Nangetty Formation|22820|6|Mentioned|p14|||Geological province: northern Perth Basin. Readily correlates with Moorhead Formation (Collie Group) in southern Perth Basin.||||||11-AUG-08
13780|Nangetty Formation|23172|4|Described|Map Legend|Permian|Permian|||||||
13780|Nangetty Formation|23174|4|Described|Fig5p8,9|Permian|Carboniferous|||||||
13780|Nangetty Formation|23279|4|Described|p10-2,Fig2p3||Asselian|(Clarke et al., 1951).||||||
13780|Nangetty Formation|23520|5|Briefly described|p11 Fig. 7|Sakmarian|Asselian|Geological Province: Perth Basin.||||||
13780|Nangetty Formation|23761|5|Briefly described|p11|||||||||
13780|Nangetty Formation|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||07-NOV-08
13780|Nangetty Formation|23816|4|Described|p229|Sakmarian|Sakmarian|Formerly known as the "Nangetty Glacial Formation". Geological Province: Perth Basin. Unconformably underlain by Tumblagooda Sandstone; conformably overlain by Holmwood Shale. Max. thickness: >1200 m.||||||18-OCT-07
13780|Nangetty Formation|23935|5|Briefly described|p17|Early Permian|Early Permian|Equivalent of Lyons Group. Geological Province: Perth Basin.||||||22-FEB-05
13780|Nangetty Formation|24058|5|Briefly described|p111 Fig. 4|Permian|Permian|Geological Basin: Perth Basin.||||||
13780|Nangetty Formation|24160|6|Mentioned|p65 fig 27, p94|Permian|Permian|Northern Perth Basin.|||||Tillitic clayey siltstone and sandstone.|
13780|Nangetty Formation|24390|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin.||||||
13780|Nangetty Formation|24410|5|Briefly described|p134 Fig. 79|Phanerozoic|Phanerozoic|Siltstone, shale, sandstone and limestone.||||||24-NOV-09
13780|Nangetty Formation|24443|5|Briefly described|Fig.30|Early Permian|Early Permian|Unconformably overlies Precambrian basement. Conformably overlain by Holmwood Shale. Geological Province: Bight Basin.||||||
13780|Nangetty Formation|29548|6|Mentioned|p230|||||||||
13780|Nangetty Formation|29721|6|Mentioned|Table 226|||||||||
13780|Nangetty Formation|30340|6|Mentioned|p2533|||Lithology||||||
13780|Nangetty Formation|30341|4|Described|p143|||||||||
13780|Nangetty Formation|30825|6|Mentioned|p32|||||||||
13780|Nangetty Formation|30948|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
13780|Nangetty Formation|30963|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
13780|Nangetty Formation|30973|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
13780|Nangetty Formation|31154|6|Mentioned|p71|||||||||
13780|Nangetty Formation|31250|6|Mentioned|p7|||Microflora||||||
13780|Nangetty Formation|31394|5|Briefly described|Fig.4|||Lower Permian.||||||18-OCT-07
13780|Nangetty Formation|31561|6|Mentioned|p18|||See also map on p20.||||||18-OCT-07
13780|Nangetty Formation|31562|6|Mentioned|p10|||Stratigraphic table||||||
13780|Nangetty Formation|31568|5|Briefly described|p19|||L.ower Permian.||||||18-OCT-07
13780|Nangetty Formation|31910|3|Fully described|Table 1|||p16.||||||18-OCT-07
13780|Nangetty Formation|32094|6|Mentioned|p382|||||||||
13780|Nangetty Formation|32337|4|Described|p24|||||||||
13780|Nangetty Formation|32648|6|Mentioned|p32|||||||||
13780|Nangetty Formation|32649|4|Described|p17|||See also Table 1.||||||18-OCT-07
13780|Nangetty Formation|32650|6|Mentioned|p89|||||||||
13780|Nangetty Formation|32714|6|Mentioned|Fig.2|||||||||
13780|Nangetty Formation|32840|6|Mentioned|Table 1|||||||||
13780|Nangetty Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
13780|Nangetty Formation|33022|6|Mentioned|p261|||Palaeomagnetism||||||
13780|Nangetty Formation|33052|6|Mentioned|p514|||Sakmarian. See also Fig.1||||||
13780|Nangetty Formation|33386|6|Mentioned|Fig.7|||||||||
13780|Nangetty Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
13780|Nangetty Formation|34287|6|Mentioned|p123|||||||||
13780|Nangetty Formation|34841|6|Mentioned|Fig.2|||||||||
13780|Nangetty Formation|35282|6|Mentioned|Fig.2|||See also Fig.26.||||||
13780|Nangetty Formation|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
13780|Nangetty Formation|35873|6|Mentioned|p75|||||||||
13780|Nangetty Formation|36199|6|Mentioned|p2|||||||||
13780|Nangetty Formation|36253|6|Mentioned|p131|||||||||
13780|Nangetty Formation|36257|6|Mentioned|Table 2.1|||||||||
13780|Nangetty Formation|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
13780|Nangetty Formation|36293|2|Defined|p83|Sakmarian|Sakmarian|||||||
13780|Nangetty Formation|36596|6|Mentioned|Text Fig.2|||||||||
13780|Nangetty Formation|36718|6|Mentioned|p459|||||||||
13780|Nangetty Formation|36872|6|Mentioned|p72|||||||||
13780|Nangetty Formation|36890|3|Fully described|p230|||Formerly "Nangetty Glacial Formation".||||||18-OCT-07
13780|Nangetty Formation|36899|6|Mentioned|p1089|||||||||
13780|Nangetty Formation|37104|6|Mentioned|Fig.3|||||||||
13780|Nangetty Formation|37295|6|Mentioned|p52|||||||||
13780|Nangetty Formation|37298|6|Mentioned|Fig.1|||||||||
13780|Nangetty Formation|37308|5|Briefly described|Fig.3|||||||||
13780|Nangetty Formation|37812|6|Mentioned|p651|||||||||
13780|Nangetty Formation|37915|3|Fully described|p459|||||||||
13780|Nangetty Formation|37920|6|Mentioned|p454|||||||||
13780|Nangetty Formation|37921|6|Mentioned|p463|||||||||
13780|Nangetty Formation|37926|6|Mentioned|p500|||||||||
13780|Nangetty Formation|38998|4|Described|p20|||See also p21.||||||18-OCT-07
13780|Nangetty Formation|39307|6|Mentioned|p44|||||||||
13780|Nangetty Formation|39854|6|Mentioned|p18|||||||||
13780|Nangetty Formation|40340|5|Briefly described|p13|||||||||
13780|Nangetty Formation|40341|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
13780|Nangetty Formation|40343|5|Briefly described|p10|||||||||
13780|Nangetty Formation|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
13780|Nangetty Formation|40347|5|Briefly described|p23|||Mention p20.||||||18-OCT-07
13780|Nangetty Formation|40636|6|Mentioned|p44|||||||||
13780|Nangetty Formation|40992|6|Mentioned|Fig.5|||||||||
13780|Nangetty Formation|41172|6|Mentioned|p116|||||||||
13780|Nangetty Formation|41195|6|Mentioned|Fig.2|||||||||
13780|Nangetty Formation|41271|6|Mentioned|p209|||||||||
13780|Nangetty Formation|41284|6|Mentioned|p89|||||||||
13780|Nangetty Formation|41728|5|Briefly described|p442|||||||||
13780|Nangetty Formation|41729|6|Mentioned|p453|||||||||
13780|Nangetty Formation|42309|6|Mentioned|p256|||||||||
13780|Nangetty Formation|42547|4|Described|p105|||In the Perth Basin.||||||18-OCT-07
13780|Nangetty Formation|42711|6|Mentioned|p19|||Geological province: Perth Basin. Equivalent to Shotts Formation in the Collie Basin.||||||
13780|Nangetty Formation|43015|5|Briefly described|Table 1,p319|||||||||
13780|Nangetty Formation|43031|4|Described|p11,Fig.2.|||||||||
13780|Nangetty Formation|43067|5|Briefly described|p119|||see also Fig.12,p124||||||
13780|Nangetty Formation|43296|5|Briefly described|Map Legend||Permian|||||||
13780|Nangetty Formation|43495|4|Described|6-25||Asselian|||||||
13780|Nangetty Formation|44144|4|Described|p508 Tb. 4-21, p509 Fig.4-145, p510-512|Asselian|Asselian|May extend into Carboniferous. Type area: Nangetty Hills; no Type Section designated. 1500m thick glacial marine and glaciofluvial or lacustrine deposits. Erratics derive from Precambrian rocks, Tumblagooda Sandstone, Morawa Lavas and Noondine Chert, implying ice movement towards NNW.||||Unconformably overlies Tumblagooda Sandstone. Is overlain gradationally by Holmwood Shale.|Tillite, shale (sometimes varved), sandstone and conglomerate; some large clasts are striated.|
13780|Nangetty Formation|44237|14|Not recorded|p.200,201|||Fig.2.||||||
13780|Nangetty Formation|44998|14|Not recorded|p.67|||||||||
13780|Nangetty Formation|45016|14|Not recorded|p.14,31|||Continuous with Lyons Group.||||||
13780|Nangetty Formation|46849|6|Mentioned|Fig. 6|||||||||
13780|Nangetty Formation|48615|14|Not recorded|Fig.4,6|||||||||
13780|Nangetty Formation|49644|5|Briefly described|Table|||||||||
13780|Nangetty Formation|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
13780|Nangetty Formation|50107|5|Briefly described|map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
13780|Nangetty Formation|60376|5|Briefly described|p17 Fig. 4.|Early Permian|Early Permian|Geological Province: Perth Basin. Overlain by Holmwood Shale.||||||07-FEB-11
13780|Nangetty Formation|60377|5|Briefly described|p61 Fig. 3, p64|Asselian|Asselian|Overlain by Holmwood Shale. Geological Province: Perth Basin. Glacial Marine depositional environment.||||||07-FEB-11
13780|Nangetty Formation|60386|5|Briefly described|p291, 297, 309|Asselian|Visean|Perth Basin. Glacially influenced. Post-rift transition phase following Alice Springs Orogeny. Non-marine.|||||Glacial deposits.|
13780|Nangetty Formation|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||11-APR-08
13780|Nangetty Formation|61546|6|Mentioned|p382, p385 Fig.5, p386. |Early Permian|Early Permian|Glacigene sediments.||||Is overlain by Holmwood Shale.||
13780|Nangetty Formation|61811|4|Described|p3 Fig.2, pp22-28, p36, p64.|Early Permian|Carboniferous|Northern Perth Basin. Deposition from debris flows. Includes clasts from Yandanooka and Moora Groups, 100 -250 km to the south, and some from the Tumblagooda Sandstone. No type section proposed, but type area is Nangetty Hills.|||Includes Wicherina Member.|Unconformably overlies Tumblagooda Sandstone. Is overlain by Holmwood Shale.|Includes diamictite, interbedded with highly-deformed fine- to medium-grained sandstone, and mudstone; many striated and facetted clasts.|
13780|Nangetty Formation|62113|3|Fully described|pp618-621, pp623-624, pp629-630.      |Sakmarian|Carboniferous|Oldest part of Perth Basin fill; deposited in a deep-water marine, fiord-like environment. 1.5 km thick. Contains plant microfossils Spelaeotriletes ybertii to Pseudoreticulatispora confluens zones indicating Serpukovian - mid-Sakmarian age (Blackhouse, 1998; Eyles et al, 2002). Low hydrocarbon-generation potential.|||Includes Wicherina Member.|Interfingers with Wicherina Member. Is overlain by Holmwood Shale.|A succession of massive and laminated marine mudstones with striated dropstones; sandy mudstone matrix with variable clast content.|
13780|Nangetty Formation|64580|4|Described|map legend|Early Permian|Mississippian|Diamictite, shale (in places varvoid), conglomerate, sandstone.||||||09-DEC-08
13780|Nangetty Formation|64630|5|Briefly described|p31 Fig.2, p34|Sakmarian|Visean|Province: Northern Perth Basin. Underlies the Holmwood Shale. Palynology age: G. maculosa to P. confluens. Lithology: predominantly fossiliferous marine mudstone showing clear glacial features.||||||24-NOV-09
13780|Nangetty Formation|64635|5|Briefly described|p4 Fig.3, p17-18    |Permian|Carboniferous|Glacigene deposits; thickness to 1500 m. Typically contains Asselian-Sakmarian palynomorphs and Middle to Late Carboniferous palynomorphs in places.|||Includes Wicherina Member.|Is overlain by Holmwood Shale.|Consists of shale, sandstone, conglomerate, and minor tillite. Massive facies predominate but crude horizontal stratification, rafts of deformed sandstone, and conglomerate are common.|
13780|Nangetty Formation|64972|5|Briefly described|p615, p617 Fig. 4, p617 Fig. 5, p619|Early Permian|Late Carboniferous|Geological Province: Perth Basin. Shale and pebbly siltstone.||||||
13780|Nangetty Formation|64974|6|Mentioned|p144 Fig. 3||Asselian|Geological Province: Perth Basin.||||||24-JUN-09
13780|Nangetty Formation|64981|6|Mentioned|p670.|||Perth Basin. Regional transgression at the base of this unit, the Lyons Group in Carnarvon Basin and the Mosswood Formation in Perth Basin may be coeval with partial melting of extensive Carboniferous ice caps.||||||
13780|Nangetty Formation|65382|5|Briefly described|p714|Mississippian|Mississippian|Glaciomarine formation located in the northern Perth Basin. Contains the G. maculosa palynoflora assemblage which lies between the A. largus (335 Ma) and the S. ybertii (323 Ma) assemblages.||||||
13780|Nangetty Formation|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin.||||Is overlain by High Cliff Sandstone.|Glacial diamictite.|
13780|Nangetty Formation|67340|6|Mentioned|p6, 25|Carboniferous|Carboniferous|Northern Perth Basin. Thermal rock properties.|||Wicherina Member.|||
13780|Nangetty Formation|67354|5|Briefly described|p88, p106.|||Northern Perth Basin. Equivalent to Treachery Formation (Bonaparte Basin): both have G. confluens Oppel Zone, and evidence of ice-transported debris.|||Includes Wicherina Member.|||
13780|Nangetty Formation|67925|5|Briefly described|Ch3 p15, Ch4 p8 fig 2|Lower Permian|Lower Permian|Northern and central Perth Basin.||||Unconformably overlies the Tumblagooda Sandstone. Overlain by the Holmwood Shale.||
13780|Nangetty Formation|69029|6|Mentioned|p332|||Of Perth Basin.||||Overlain by Mosswood Formation.||
13780|Nangetty Formation|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p11|Early Permian|Early Permian|Perth Basin. See also Ch2 p34, Ch2 p45, Ch2 p47-p49, 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 Wicherina Sandstone.|Overlain by the Holmwood Shale.|Glacial debris.|
13780|Nangetty Formation|69547|6|Mentioned|p182,193|Sakmarian|Asselian|northern Perth Basin.||||||
13780|Nangetty Formation|69583|5|Briefly described|p130, Plate 3.|Paleozoic|Paleozoic|Perth Basin.|||||Diamictite, shale (locally varved), conglomerate, sandstone.|
13780|Nangetty Formation|70097|5|Briefly described|p2, p20 Fig.4|Sakmarian|Asselian|Northern Perth Basin. Irwin Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.|||Wicherina Member|Is overlain by Holmwood Shale.|Glacial basin fill. Includes shale and sandstone.|12-SEP-17
13780|Nangetty Formation|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Is overlain conformably by Holmwood Shale.||
13780|Nangetty Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Northern Perth Basin.||||Overlain by the Holmwood Shale.||
13780|Nangetty Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Sakmarian|Pennsylvanian|Perth Basin. Formed during Gondwana breakup along the western margin.|323.2290.1 Ma (biostrat)||||Diamictite, shale (locally varvoid), conglomerate, sandstone.|
13780|Nangetty Formation|70826|6|Mentioned|p6 tbl 3|Early Permian|Late Carboniferous|Perth Basin.||||||
13780|Nangetty Formation|71146|5|Briefly described|p6|Sakmarian|Late Carboniferous|Perth Basin.||||Overlain by the Holmwood Shale.|Mudstone.|
13780|Nangetty Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, sandstone, conglomerate, tillite|
13780|Nangetty Formation|71269|5|Briefly described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|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.|323.2-290.1 Ma (biostrat)||||Diamictite, shale (locally varvoid), conglomerate, sandstone|
13780|Nangetty Formation|71781|5|Briefly described|p56, Plate 3||Permian|||||||
13780|Nangetty Formation|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Pennsylvanian|Carboniferous-Permian glacigene rocks, Perth Basin.  Age from biostratigraphy.|||||Diamictite, shale (locally varvoid), conglomerate, sandstone.|
13780|Nangetty Formation|72258|5|Briefly described|p127, p129|Cisuralian|Cisuralian|Of Perth Basin. Records the late Paleozoic ice age for which no Zircon U-Pb data currently exists.||||Overlain by Holmwood Shale. Laterally grades into Mosswood Formation.||15-JAN-20
13780|Nangetty Formation|72505|5|Briefly described|p890|Asselian|Carboniferous|Perth Basin. Correlated with the P. Confluens and Microbaculispora tentula zones.||||Overlain by the Holmwood Shale.||
13780|Nangetty Formation|72910|6|Mentioned|p4 Fig.3.|Asselian|Asselian|Shown as part of the Northern Perth Basin.||||Underlies Holmwood Shale and is partly laterally equivalent to Lyons Group.||
13780|Nangetty Formation|73117|6|Mentioned|p15, p35|Asselian|Gzhelian|Perth Basin, Irwin Terrace. Glacigene. Contains Cycadopites cymbatus.||||Overlain by Holmwood Shale.||
13780|Nangetty Formation|73184|6|Mentioned|p200, p201 Fig.12|Sakmarian|Visean|Perth Basin. Partly coeval with the Reeves Formation. Only sedimentological evidence for ca Bashkirian glaciation.|||||Glaciomarine deposits, contains speculated Carboniferous glacial deposits.|
13780|Nangetty Formation|73484|6|Mentioned|p476 Fig.3|Cisuralian|Cisuralian|Perth Basin. Glaciogene.||||Underlies Holmwood Shale||
13780|Nangetty Formation|73513|5|Briefly described|p30 Fig.2, p31, p33|Asselian|Asselian|Perth Basin. Glacial to pro-glacial marine setting.||||Underlies Holmwood Shale|Fluvial-glacial unit.|
13780|Nangetty Formation|73623|5|Briefly described|p1, 3-4, 6, 14, 16, 18|Sakmarian|Gzehelian|Clarke et al. (1951). Irwin Basin. Estimated maximum thickness of c.1000m. The boundary with the overlying Holmwood Shale marks the last appearance of glacially influenced sediment in the Irwin Basin.||||Is overlain conformably by Holmwood Formation. Correlative of Lyons Group.|Glacigenic; mainly glacial rock flour with interspersed diamictites. Contains sandy shale overlying diamictite in its upper section.|
13791|Nannyarra Sandstone|6944|6|Mentioned|p571 Fig.2.|Middle Devonian|Middle Devonian|Named thus in Fig.2 (after Hocking et al., 1987). Throughout the text, the authors refer to this unit as Nannyarra Formation. Nearshore marine depositional environment.||||||27-OCT-14
13791|Nannyarra Sandstone|12471|6|Mentioned|p475 Fig.2. |Middle Devonian|Middle Devonian|Patchy sedimentation of a transgressive sand that locally onlaps various older units.||||Is overlain by Gneudna Formation.||
13791|Nannyarra Sandstone|12729|4|Described|p.11, 28, 31-2; Figs. 4, 6, 9, 10, 23-4.|Givetian|Givetian|Up to 190 m thick. Type section (57m thick) near Williambury Homestead. Deposition: low-energy, shallow-marine, intertidal, marks start of a major transgression. Nth wells yielded Givetian-Frasnian optivus-triangulatus spore-pollen Zone and CRAE GRH 1 giving the Eifelian-Givetian devonicusnaumovae or velata-langii Zone.||||Conformably underlies the Gneudna Formation, unconformably overlies Dirk Hartog Group in Pendock 1.|Predominantly sandstone with minor siltstone.|
13791|Nannyarra Sandstone|12731|5|Briefly described|p590 Fig.2.|Middle Devonian|Middle Devonian|Potential hydrocarbon reservoir with Gneudna Formation as a seal.||||Is overlain by Gneudna Formation.|Basal transgressive sands.|
13791|Nannyarra Sandstone|12733|5|Briefly described|p554 Fig.2.|Middle Devonian|Middle Devonian|Givetian.||||Is overlain by Gneudna Formation.|Shallow-marine transgressive sandy sediments.|
13791|Nannyarra Sandstone|13615|3|Fully described|p4, p6-8, 16,34, 79-81, p83, p104 App. 3|Frasnian|Givetian|Peedamullah Shelf. Up to 150m thick. . Type section occurs 6km south of Gneudna Well, Williambury Homestead; 23deg58'10"S 115deg12'40" E. Barren of  fossils in outcrop. Age inferred. Deposited in a mainly shoreface environment. See also Plates 2, 3. See also Nannyarra Formation p16.|c. 378 Ma|||Unconformably overlies the Tumblagooda Sandstone. Conformably overlain by the Gneudna Formation.|Sandstone, lithic to quartz wacke, arenite and minor siltstone and claystone.|01-MAY-19
13791|Nannyarra Sandstone|14228|5|Briefly described|p5 fig 2, p6 fig3, p7, p18-21, p26|Givetian|Eifelian|Gascoyne Platform and Merlinleigh Sub-basin. Up to 190 m thick. Good reservoir characteristics.||||Overlies Dirk Hartog Group at an angle. Grades upwards into Gneudna Formation.|Light-grey, brown, medium- to coarse-grained sandstone; minor green to brown shale, chloritic, micaceous.|
13791|Nannyarra Sandstone|22814|5|Briefly described|fig2|Devonian|Devonian|||||||
13791|Nannyarra Sandstone|23311|5|Briefly described|map legend|Early Devonian|Early Devonian|||||||
13791|Nannyarra Sandstone|23312|5|Briefly described|map legend||Early Devonian|||||||
13791|Nannyarra Sandstone|23403|4|Described|p7|Early Carboniferous|Middle Devonian|Consists of coarse- to fine-grained, variably sorted, thin-bedded sandstone.  Geological Province: Gascoyne Complex.||||||24-NOV-09
13791|Nannyarra Sandstone|23572|4|Described|p8 Fig. 6, p11|Givetian|Givetian|Geological Province: Carnarvon Basin. Overlying Unit: Gneudna Formation (conformable). Max. thickness: 214m.||||||
13791|Nannyarra Sandstone|23726|5|Briefly described|p29|Devonian|Devonian|Overlying unit Gneudna Formation. Geological Province: Carnarvon Basin.||||||
13791|Nannyarra Sandstone|23935|5|Briefly described|p11 Fig.7|Givetian|Givetian|Conformably overlian by Gneudna Formation. Geological Province: Southern Carnarvon Basin.||||||
13791|Nannyarra Sandstone|24390|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
13791|Nannyarra Sandstone|36902|6|Mentioned|p22|||||||||
13791|Nannyarra Sandstone|37295|6|Mentioned|p51|||Proposed usage.||||||
13791|Nannyarra Sandstone|38482|6|Mentioned|p22|||||||||
13791|Nannyarra Sandstone|40617|6|Mentioned|Fig.1|||||||||
13791|Nannyarra Sandstone|40992|6|Mentioned|Fig.8|||||||||
13791|Nannyarra Sandstone|41271|3|Fully described|p43|||||||||
13791|Nannyarra Sandstone|41438|6|Mentioned|p98|||||||||
13791|Nannyarra Sandstone|41441|6|Mentioned|p151|||||||||
13791|Nannyarra Sandstone|41443|4|Described|p159|||||||||
13791|Nannyarra Sandstone|41492|6|Mentioned|p118|||||||||
13791|Nannyarra Sandstone|41512|6|Mentioned|p29|||||||||
13791|Nannyarra Sandstone|42030|3|Fully described|p744 p96|||||||||
13791|Nannyarra Sandstone|42116|5|Briefly described|p22|||See also Fig.9||||||
13791|Nannyarra Sandstone|43566|6|Mentioned|p414|||||||||
13791|Nannyarra Sandstone|49942|4|Described|p4 Fig.3, p9|Late Devonian|Middle Devonian|Conformably overlain by Gneudna Formation. Sandstone and minor siltstone deposited in a shallow marine to coastal environment. Max. thickness: 190 m. Geological Province: Gascoyne Platform.||||||
13791|Nannyarra Sandstone|50085|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
13791|Nannyarra Sandstone|60384|5|Briefly described|p244, p243 Fig 2a, p260 table 2|Late Devonian|Middle Devonian|Southern Carnarvon Basin. Shallow marine to coastal sandstone.||||||
13791|Nannyarra Sandstone|60725|5|Briefly described|p29 Fig.2; p30; p33-37; p39.|Givetian|Eifelian|Reservoir rocks.|||||Shallow-marine transgressive sand.|10-MAY-17
13791|Nannyarra Sandstone|61023|5|Briefly described|p34 Fig. 14|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
13791|Nannyarra Sandstone|64580|6|Mentioned|map legend|||Devonian succession, Southern Carnarvon Basin.||||||15-DEC-08
13791|Nannyarra Sandstone|64972|6|Mentioned|p617 Fig. 5|Devonian|Devonian|||||||
13791|Nannyarra Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes green grey mottled sandstone/siltstone.|
13791|Nannyarra Sandstone|67200|5|Briefly described|p7 fig 5|Devonian|Devonian|Thermal conductivity of 2.50 W/mK. See also p18 table 1, p48, p51, p55, app 2 p6.||||overlain by Gneudna Formation|Trough and planar cross bedded sandstone and siltstone.|
13791|Nannyarra Sandstone|69011|5|Briefly described|Map Legend|Devonian|Devonian|Southern Carnarvon Basin.||||Overlain by the Gneudna Formation.|Comprises fine- to coarse-grained sandstone; minor siltstone and claystone; local basal conglomerate.|
13791|Nannyarra Sandstone|69029|6|Mentioned|p326,328|Givetian|Emsian|Of onshore Carnarvon Basin.||||Overlain by Gneudna Formation. Underlain by Sweeney Mia Formation.||
13791|Nannyarra Sandstone|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Late Devonian|Middle Devonian|Carnarvon Basin. Deposited as part of marine transgressive cycle in a low-energy, shallow marine or intertidal environment. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p55, Ch3 p67-p68, Ch3 p73.||||Conformably overlain by the Gneudna Formation.|Sandstone and minor amounts of siltstone.|
13791|Nannyarra Sandstone|69297|4|Described|p246, p249, p250|Middle Devonian|Middle Devonian|Gascoyne Sub-basin of the Carnarvon Basin. Deposited in a shallow marine to coastal environment. Oil stains have been detected in this unit.||||Unconformably overlies the Sweeney Mia Formation. Overlain by the Gneudna Formation.|Sandstone.|
13791|Nannyarra Sandstone|70138|5|Briefly described|Map legend.|Devonian|Devonian|Southern Carnarvon Basin.||||Overlies Moorarie Supersuite. Is overlain by Gneudna Formation.|Fine- to coarse-grained sandstone; minor siltstone and claystone; local basal conglomerate.|
13791|Nannyarra Sandstone|70795|4|Described|100k_geologyp_lut.csv|Frasnian|Givetian|Also 100k_interpgeop_lut.csv|388-380 Ma||||Fine- to coarse-grained sandstone; minor siltstone and claystone; local basal conglomerate.|
13791|Nannyarra Sandstone|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Southern Carnarvon Basin.||||||
13791|Nannyarra Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone, limestone|
13794|Nanutarra Formation|23311|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group.||||||
13794|Nanutarra Formation|23325|6|Mentioned|map legend|Cretaceous|Cretaceous|||||||
13794|Nanutarra Formation|23403|5|Briefly described|p8|||||||||
13794|Nanutarra Formation|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
13794|Nanutarra Formation|23726|5|Briefly described|p70|Early Cretaceous|Early Cretaceous|Overlying unit Mardie Greensand. Geological Province: Carnarvon Basin.||||||
13794|Nanutarra Formation|23815|4|Described|p295|Early Cretaceous|Late Jurassic|Geological Province: Carnarvon Basin. Overlying unit: Yarraloola Conglomerate (conformable). Max. thickness: 75 m. Fossiliferous.||||||14-DEC-04
13794|Nanutarra Formation|24160|5|Briefly described|p36|Early Cretaceous|Early Cretaceous|Not classified as part of Winning Group.||||Underlies part of Birdrong Sandstone. Grades laterally into Windalia Radiolarite.|Clay-sand siliciclastic sequence.|
13794|Nanutarra Formation|30549|6|Mentioned|p26|||||||||
13794|Nanutarra Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
13794|Nanutarra Formation|33450|6|Mentioned|p11|||See Fig.5||||||
13794|Nanutarra Formation|34066|6|Mentioned|p12|||Cretaceous||||||
13794|Nanutarra Formation|35144|6|Mentioned|p4|||||||||
13794|Nanutarra Formation|36890|3|Fully described|p295|||||||||
13794|Nanutarra Formation|36902|6|Mentioned|p22|||||||||
13794|Nanutarra Formation|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
13794|Nanutarra Formation|37422|6|Mentioned|p6|||||||||
13794|Nanutarra Formation|38482|6|Mentioned|p22|||See also Table 10.||||||
13794|Nanutarra Formation|38589|6|Mentioned|p48|||||||||
13794|Nanutarra Formation|38776|6|Mentioned|p37|||||||||
13794|Nanutarra Formation|39158|4|Described|p38|||||||||
13794|Nanutarra Formation|39427|4|Described|Table 1|||||||||
13794|Nanutarra Formation|40617|6|Mentioned|p18|||||||||
13794|Nanutarra Formation|41271|3|Fully described|p143|||||||||
13794|Nanutarra Formation|41438|6|Mentioned|p108|||||||||
13794|Nanutarra Formation|41441|6|Mentioned|p153|||||||||
13794|Nanutarra Formation|41443|6|Mentioned|p164|||||||||
13794|Nanutarra Formation|41446|3|Fully described|p215|||||||||
13794|Nanutarra Formation|42116|5|Briefly described|p51|||See also Fig.18||||||
13794|Nanutarra Formation|42260|6|Mentioned|p98|||||||||
13794|Nanutarra Formation|42598|3|Fully described|P 93, P 33|late Neocomian||||||||
13794|Nanutarra Formation|43442|6|Mentioned|p61|||Northern Carnarvon Basin||||||
13794|Nanutarra Formation|44376|14|Not recorded|p10|||||||||
13794|Nanutarra Formation|44477|4|Described|p.15, Table 1||Mesozoic|SF/50-6.||||||
13794|Nanutarra Formation|44478|14|Not recorded|map legend||Cretaceous|||||||
13794|Nanutarra Formation|44481|5|Briefly described|map legend||Cretaceous|||||||
13794|Nanutarra Formation|44999|14|Not recorded|?|||||||||
13794|Nanutarra Formation|45005|14|Not recorded|?|||||||||
13794|Nanutarra Formation|45011|14|Not recorded|p53,64-68,77,81,89,||Neocomian|p97,98,102,104. Correlated with Mullaman Beds.||||||
13794|Nanutarra Formation|45015|5|Briefly described|map legend|Late Jurassic|Late Jurassic|Geological Province: Carnarvon Basin.||||||31-MAY-06
13794|Nanutarra Formation|45110|6|Mentioned|p141|||||||||
13794|Nanutarra Formation|61958|5|Briefly described|Map sheet 1|Late Jurassic|Late Jurassic|||||||21-MAR-06
13794|Nanutarra Formation|64580|4|Described|map legend||Early Cretaceous|Silty, fine- to coarse-grained, poorly sorted sandstone, siltstone, claystone, greensand, minor conglomerate.||||||09-DEC-08
13794|Nanutarra Formation|64973|6|Mentioned|p504|||Misspelt or obsolete name. The original use of the name was not intended to be formal.||||||16-JUN-09
13794|Nanutarra Formation|67200|5|Briefly described|p8 fig 6, |Cretaceous|Cretaceous|||||Overlain by Muderong Shale|Parallel and trough cross bedded, interbedded sandstone, siltstone and conglomerate.|
13794|Nanutarra Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Yarraloola Conglomerate|||Silty, fine- to coarse-grained, poorly sorted sandstone, siltstone, claystone, greensand, minor conglomerate.|
13794|Nanutarra Formation|69185|4|Described|GEOL_LUT_CSV files||Early Cretaceous|Of Northern Carnarvon Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Silty, fine- to coarse-grained, poorly sorted sandstone, siltstone, claystone, greensand, minor conglomerate|
13794|Nanutarra Formation|70127|5|Briefly described|Map legend|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||||Sandstone, siltstone, lesser pebble to cobble conglomerate; texturally immature.|
13794|Nanutarra Formation|70138|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||||Sandstone, siltstone, lesser pebble to cobble conglomerate; texturally immature.|
13794|Nanutarra Formation|70795|4|Described|100k_geologyp_lut.csv|Aptian|Berriasian|Also 2_5m_interpgeop15_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|||||Sandstone, siltstone, lesser pebble to cobble conglomerate; texturally immature.|
13794|Nanutarra Formation|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
13794|Nanutarra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, greensand, siltstone, shale|
13794|Nanutarra Formation|71273|5|Briefly described|Map legend.|Cretaceous|Cretaceous||145-113 Ma.||||Sandstone, siltstone, lesser pebble to cobble conglomerate; texturally immature.|
13794|Nanutarra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Berriasian|Northern Carnarvon Basin. Max age inferred, min age from biostratigraphy.|||||Sandstone, siltstone, lesser pebble to cobble conglomerate; texturally immature.|
13794|Nanutarra Formation|72758|5|Briefly described|p8 Tb.1, p54.|Cretaceous|Cretaceous|Occuring as small mesas and buttes northwest Wyloo map sheet area.||||Unconformably overlies Mount Minnie Group.|Ferruginous sandstone and conglomerate, siltstone and some fissile mudstone.|
13856|Nardoopiquithanna Adamellite|35641|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
13856|Nardoopiquithanna Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
13856|Nardoopiquithanna Adamellite|39697|3|Fully described|p38|||||||||
13856|Nardoopiquithanna Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||125 sq. km. Post-tectonic granitoid.||Yule Granitoid Complex|||Biotite monzogranite.|
13861|Narmia Member|30565|6|Mentioned|p120|||||||||
13861|Narmia Member|34008|6|Mentioned|p69|||Scythian.  See also P75||||||
13894|Narracoota Formation|12099|3|Fully described|p676-682, 685-6, Fig.2, 4,7, 9 Tab.1|Orosirian|Orosirian|New or redefined unit by Occhipinti et al. (1997). Parts formerly called Narracoota Volcanics by Gee (1987) and Gee and Grey (1993) and placed in the Glengarry Group. Forms the bulk of the Bryah Group. Emplaced in an oceanic and continental setting. Estimated thickness of 6 km. Pb-Pb isochron age.|1920+/-35 Ma (Pb-Pb isochron: Windh 1992).|Unit in Bryah Group.||Unconformably overlies and locally interfingers with the Karalundi Formation. Disconformably overlain by Ravelstone Formation. Locally in faulted contact with Padbury Group, Horseshoe Formation.|Metamorphosed peridotitic and high-Mg basalt, basaltic hyaloclastite, mafic pyroclastic rocks, mafic intrusive rocks, and mafic and ultramafic schist.|04-MAR-13
13894|Narracoota Formation|22694|5|Briefly described|p7|||Bryah Group||||||
13894|Narracoota Formation|22940|4|Described|p13, Fig.1 p3|Paleoproterozoic|Paleoproterozoic|Pb-Pb model age 1920+/-35 Ma (Windh, 1992). See also Fig.6 p14, p10. of Bryah Group.||||||07-NOV-08
13894|Narracoota Formation|23151|5|Briefly described|p67|||of Bryah Group.||||||
13894|Narracoota Formation|23153|6|Mentioned|p83|||||||||
13894|Narracoota Formation|23592|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Age: 1920+/-35 Ma (Pb-Pb isochron). Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
13894|Narracoota Formation|23593|5|Briefly described|p2 Fig 1|||Of Bryah Group. Geological Province: Bryah Basin||||||
13894|Narracoota Formation|23597|5|Briefly described|p11|||Of Bryah Group||||||
13894|Narracoota Formation|23600|5|Briefly described|p4 Fig 2|||Of Bryah Group. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|23744|4|Described|p11|Statherian|Statherian|Age: 1920+/- 35 Ma (Pb-Pb isochron). See also page 22. Of Bryah Group. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|23747|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Age: 1920+/-35 Ma (Pb-Pb isochron). See also page 4 Table 1. Formerly Narracoota Volcanics. Of Bryah Group. Geological Province: Bryah Basin.||||||07-NOV-08
13894|Narracoota Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin||||||
13894|Narracoota Formation|23749|4|Described|p11|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Bryah Group. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|23865|6|Mentioned|p177|||Geological Province: Yerrida Basin.||||||
13894|Narracoota Formation|23890|5|Briefly described|p21 Fig.11|||Of Bryah Group. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|24021|5|Briefly described|p3, Fig. 1|||Parent: Bryah Group.||||||
13894|Narracoota Formation|24028|6|Mentioned|p295|||||||||
13894|Narracoota Formation|42730|5|Briefly described|Fig 12, P15|||Variation on Narracoota Volcanics.||||||
13894|Narracoota Formation|43238|4|Described|p6|||of Bryah Group.||||||
13894|Narracoota Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Bryah Basin||||||07-NOV-08
13894|Narracoota Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Bryah Basin||||||07-NOV-08
13894|Narracoota Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
13894|Narracoota Formation|44927|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
13894|Narracoota Formation|49893|5|Briefly described|p2 Fig.1|||Of the Bryah Group. Mafic and ultramafic schist, and metabasaltic hyaloclastic.||||||
13894|Narracoota Formation|49896|5|Briefly described|p3 Tb. 2|||Of Windh (1992). Supersedes Narracoota Volcanics. Mafic and ultramafic schist/ metabasaltic hyaloclastite. Age: 1.92Ga depositional age (Pb-Pb).||||||
13894|Narracoota Formation|50218|5|Briefly described|p244, p252|Paleoproterozoic|Paleoproterozoic|Of the Bryah Group. Geological Province: Bryah Basin.||||||07-FEB-11
13894|Narracoota Formation|50221|5|Briefly described|p297|Paleoproterozoic|Paleoproterozoic|Of the Bryah Group. Characterised by metamorphosed mafic and ultramafic schists, basalt and gabbros.||||||07-NOV-08
13894|Narracoota Formation|50222|3|Fully described|p320 Fig. 3, p324-325|Paleoproterozoic|Paleoproterozoic|Of the Bryah Group.  Now incorporates the former Trillbar Complex (Myers, 1999).  Max. thickness: ?6000m (Pirajno and Occhipinti, 1998).  Disconformably overlain by Ravelstone Formation.  Age: >1.92Ga (Pb-Pb, Wingh, 1992).  Geol. Province: Bryah Basin.||||||07-NOV-08
13894|Narracoota Formation|50226|5|Briefly described|p420, p421 Fig. 4, p422|||Includes the former Trillbar complex of Myers (1990).  Mafic to ultramafic schist/metabasaltic hyaloclastites and volcaniclastic rocks.  Overlain by Ravelstone and Horseshoe Formations.  Geological Province: Bryah Basin.||||||24-JUN-04
13894|Narracoota Formation|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|See also Narracoota Volcanics. Of the Bryah Group. Mafic and ultramafic volcanic rocks.||||||07-FEB-11
13894|Narracoota Formation|61271|5|Briefly described|p105 Fig.1, p106|||Of the Bryah Group. Overlies the Karalundi Formation. Mafic and ultramafic schist/metabasaltic hyaloclastite.||||||
13894|Narracoota Formation|61848|5|Briefly described|p300|||Mafic and ultramafic volcanic rocks. Geological Province: Bryah Basin.||||||
13894|Narracoota Formation|62289|5|Briefly described|plate 1, p3 Fig. 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Bryah Group; metabasalt and mafic-ultramafic schist; locally pillowed with metamorphosed interflow sedimentary layers; Geol. Prov: Bryah Basin.||||||
13894|Narracoota Formation|63866|5|Briefly described|p152, p164, p168, p177|||Western Glengarry Basin. Forms the bulk of the Bryah Group. Pb-Pb isochron dates obtained for this formation probably represent mineralizing events rather than minimum depositional ages for this formation and the Bryah Group.|c. 1920 Ma (inferred depositional age)|Bryah Group|||Metamorphosed, peridotitic and high-Mg basalt, basaltic hyaloclastite, mafic pyroclastic rocks, mafic intrusive rocks and mafic and ultramafic schist.|
13894|Narracoota Formation|64580|4|Described|map legend||Paleoproterozoic|Of Bryah Group. Basaltic vent breccia, hyaloclastite; Jasperoidal chert; Metaperidotite and picrite; Metabasalt and mafic-ultramafic schist; Felsic schist; from felsic volcanic and volcaniclastic rock; Dolerite; in sills and dykes; Gabbro; microgabbro.||||||09-DEC-08
13894|Narracoota Formation|64724|5|Briefly described|p43|||Voluminous mafic and ultramafic igneous rocks near the base of the Bryah Basin.||||||
13894|Narracoota Formation|65408|5|Briefly described|pp82-83, p85|Statherian|Orosirian|Subalkaline affinity; low REE abundances. Trace- and major-element data suggest mixed MORB to oceanic-island chemical signatures. Age is of supposed syngenetic pyrite.|1920 +/- 35 Ma Pb/Pb model age (Windh 1992).|Unit in Bryah Group.|||Mafic-ultramafic volcanics and dykes, tuffs and intercalated sedimentary rocks.|
13894|Narracoota Formation|65411|5|Briefly described|p88, pp90-93.|Paleoproterozoic|Paleoproterozoic|REE geochemical analyses suggest this unit is the source of mafic epiclasts in the Beatty Park Member of the Wilthorpe Formation.||Unit in Bryah Group.|||Mafic-ultramafic volcanic rocks of oceanic origin.|
13894|Narracoota Formation|65412|5|Briefly described|pp97-103.|Paleoproterozoic|Paleoproterozoic|Bryah Basin. Volcanism has a range of MORB to oceanic island chemical signature. Is spatially associated with a positive Bouguer anomaly, suggesting a rift-related large underlying (mafic) body(ies).||Unit in Bryah Group.||Intercalated with Karalundi Formation.|Mafic-ultramafic schist, metabasaltic hyaloclastite, metabasalts of subalkaline Mg-rich tholeiitic affinity; mafic pyroclastics common.|
13894|Narracoota Formation|65418|4|Described|pp169-175.|||New name (Pirajno and Occhipinti, 1995; Pirajno and Occhipinti, in prep.); includes most of the Narracoota Volcanics of Gee (1987, 1990) and Gee and Grey (1993) but excludes the suite of mafic rocks in the SE corner of the Peak Hill 1:250 000 map sheet now included in the Killara Formation (Dawes and Le Blanc Smith, 1995). Glengarry Basin. Geochemistry and chemical weathering are detailed: overall chemistry of regolith closely reflects that of the parent rock, which may be useful in exploration and mapping.|||||Metamorphosed mafic and ultramafic volcanic rocks now preserved as tremolite-actinolite and chlorite schists; largely tholeiitic with some subvolcanic high-Mg cumulates.|21-FEB-17
13894|Narracoota Formation|65419|1|Redefined|p4 Fig.1, p30, p31, pp32-34, p42.|Paleoproterozoic|Paleoproterozoic|Incorporates units previously assigned to 'Dolerite' (MacLeod 1970), 'Basalt' (Elias et al. 1982), 'Dolerite' (Elias and Bunting 1982); corresponds in part to Narracoota Volcanics (Gee 1979, 1987 and Hynes and Gee, 1986). Tholeiitic basalts SE of Goodin Inlier and in Paroo Platform, assigned to Narracoota Volcanics by Gee and Grey (1993), are now assigned to Killara Formation, as are volcanics on eastern Glengarry and Peak Hill 1:250 000 sheets. Named after Narracoota Homestead. No type section; type area in the Mikhaburra-Cashman area, 10 to 15 km south of Narracoota Homestead. Thickness uncertain, estimated 6 km (Gee, 1979). Includes a pyrite with a Pb-Pb isochron  of 1922 +/- 35 Ma (Windh, 1992): may be the date of mineralisation, not deposition.||Unit in Bryah Group.||Overlies conformably and interfingers with Karalundi Formation. In faulted contact with Padbury Group, Horseshoe Formation and Peak Hill Schist. Is overlain disconformably by Ravelstone Formation.|Dolerite dykes and sills, hyaloclastites, local spinifex-textured komatiites, olivine cumulate; mafic schist including amphibolite and tremolite-actinolite schist; generally high-magnesium tholeiites; commonly metasomatised.|
13894|Narracoota Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Bryah Group. Metabasalt, mafic and ultramafic schists; locally plagioclase phyric; with local fragmental texture; and local metadolerite; includes volcaniclastic rock (locally coeval and interbedded with Ravelstone Formation)||||||
13894|Narracoota Formation|65913|5|Briefly described|p2 Fig.1, pp15-16. |||Formerly Narracoota Volcanics; used to include rocks now assigned to the Killara Formation. Has a dominantly oceanic geochemical signature.||Unit in Bryah Group.||||
13894|Narracoota Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Bryah Group. Basalt and mafic-ultramafic schist; locally pillowed and plagioclase-phyric; interbedded with volcaniclastic and sedimentary rock (coeval and interbedded with Ravelstone Formation).||||||
13894|Narracoota Formation|66299|4|Described|p148, p208.|Paleoproterozoic|Paleoproterozoic|Bryah Basin, Gascoyne Province.||Unit in Bryah Group.||Is in faulted contact with Kerba Granite.|Mafic and ultramafic schists; typically actinolite-tremolite(-talc-chlorite) assemblages.|
13894|Narracoota Formation|66427|6|Mentioned|p40 Fig.2||||c.2.0-1.99 Ma.|Unit in Bryah Group.|||Oceanic crust.|
13894|Narracoota Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|Bryah Basin||Bryah Group|||Basaltic vent breccia and hyaloclastite; Jasperoidal chert; Metaperidotite and picrite; ultramafic schist; Metabasalt and mafic-ultramafic schist; Dolerite; gabbro; microgabbro; pyroxenite; and serpentinized peridotite;|
13894|Narracoota Formation|69003|4|Described|p4, p11-14|||Bryah Basin, Capricorn Orogen. ?6000m thick. Interpreted as remnants of an oceanic plateau,  accreted during the Glenburgh Orogeny between c.1965 and c.1950 Ma. Hosts VHMS Cu-Au-Ag mineralisation.|c.2000 Ma.|||Overlies Karalundi Formation. Is overlain conformably by Ravelstone Formation.|Mafic-ultramafic schist, metabasaltic hyaloclastite.|
13894|Narracoota Formation|69010|5|Briefly described|Map Legend||Orosirian|Bryah Basin. Two unnamed facies are mapped separately: dolerite sills and dykes; and sericitic felsic volcanic rock, locally porphyritic with equant quartz phenocrysts, weakly to strongly foliated.|< 2014 Ma|Of the Bryah Group.|||Comprises basalt, locally pillowed and plagioclase-phyric, and mafic-ultramafic schist; interbedded with volcaniclastic and sedimentary rocks; metamorphosed.|24-APR-14
13894|Narracoota Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Bryah Basin.|c. 2000 Ma|Of the Bryah Group.|Includes Trillbar Member.|Coeval and interbedded with the Ravelstone Formation.|Metabasalt and mafic-ultramafic schist; locally pillowed and plagioclase-phyric; interbedded with volcaniclastic and sedimentary rock.|06-MAY-14
13894|Narracoota Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Bryah Group||Coeval and interbedded with Ravelstone Formation.|Basalt and mafic-ultramafic schist interbedded with volcaniclastic and sedimentary rock. Jasperoidal Chert, talc-chlorite-quartz schist, Actinolite schist, dolerite sills and dykes, siltstone, biotite-chlorite slate.|
13894|Narracoota Formation|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Bryah Basin. Coeval with Ravelstone Formation.||Bryah Group.||Interbedded with Ravelstone Formation.|Metabasalt and mafic-ultramafic schist.|
13894|Narracoota Formation|69596|5|Briefly described|p10-11|||Bryah Basin.||||Is overlain disconformably by Ravelstone Formation.|Mafic to ultramafic intrusive and volcaniclastic rocks including peridotitic and high-Mg basalt, mafic to ultramafic schists, pillow-structured metabasalts.|
13894|Narracoota Formation|69740|5|Briefly described|p652, 663, 676|Paleoproterozoic|Paleoproterozoic|Capricorn Orogenic Belt. Suprasubduction zone-type ophiolite; in back-arc.|2.0 Ga.||||Pillow basalt, sheeted dyke complex, layered mafics and ultramafics, boninites.|
13894|Narracoota Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv,  West Australian Craton, Bryah Basin|2014-1920 Ma|Bryah Group|||Basalt, locally pillowed and plagioclase phyric, ultramafic and mafic schist, jasperoidal chert, siltstone; local biotite-chlorite slate, sericitic felsic volcanic rock; dolerite, basalt, ultramafic and mafic schist, chlorite slate.|
13894|Narracoota 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, site_lithology.csv, Glengarry100_2645_stratig.pdf.|2014  1920 Ma (inferred)|Bryah Group, lower|||Basalt, locally pillowed and plagioclasephyric, and maficultramafic schist; interbedded with volcaniclastic and sedimentary rocks; metamorphosed.|
13894|Narracoota Formation|70804|4|Described|p2, p6-p17, p19, p24-p26|Orosirian|Orosirian|Bryah Basin. Replaces the obsolete Narracoota Volcanics. Estimated thickness of up to 6km. Rocks of this unit are affected by sea-floor metasomatism and regional metamorphism. Geochemistry, petrography and lithology discussed in detail. SHRIMP age derived from a chert lense directly underlying the Beatty Park Member of the overlying Wilthorpe Formation. Hosts the old Mikhaburra gold mine. See also p28, p37-p38, p41-p44, p47-p48, plate 1.|c. 1996 +/- 35 Ma (SHRIMP U-PB)|Bryah Group||Conformably overlies the Karalundi Formation. Disconformably overlain by and locally interfingers with the Ravelstone Formation. Overlain by the Beatty Park Member.|Tholeiitic extrusive and intrusive rocks and subordinate ultramafic units, intercalated with minor jasperoidal chert units and clastic sedimentary rocks.|
13894|Narracoota Formation|70814|5|Briefly described|p48|||Bryah Basin. Hosts the Fortnum gold mine, DeGrussa copper-gold mine and the Horseshoe Lights copper-gold deposit.||||Overlain by the Thaduna Formation.||05-MAY-23
13894|Narracoota Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite, peridotite, pyroxenite, basalt, mafic and ultramafic schist|
13894|Narracoota 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.|||Basalt, locally pillowed and plagioclase-phyric, and mafic--ultramafic schist; interbedded with volcaniclastic and sedimentary rocks; metamorphosed|
13894|Narracoota Formation|71468|4|Described|p24-36,38|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Bryah Sub-basin. Age is constrained to 2030-1990 Ma, primarily from the DeGrussa VHMS deposit. Zircons from dolerite dykes were dated at 2003+\-7, 1999+\-7 and 1991+\-7 Ma,  interpreted to be coeval with  Narracoota Formation (Hawke et al., 2015). 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||Overlain by, and laterally grades into Ravelstone Formation, and Horseshoe Formation. Underlain by, and interfingers with Karalundi Formation.|Mafic volcanic rocks, including massive and pillowed basalt (including High-Mg basalts) and hyaloclastite.|20-AUG-19
13894|Narracoota Formation|71484|4|Described|p122-123,125-128,134-139|Orosirian|Orosirian|Geological province:Of Bryah Basin. Up to 7km thick in the central part of the basin, based on gravity modelling (Pirajno and Occhipinti, 1998). Underwent heterogeneous deformation; dominated by pervasive mafic schists N of Murchison Fault, and massive undeformed basaltic rocks S of Murchison Fault. Probably includes E-trending dolerite dykes with ages at 2003+\-7 Ma, 1999+\-7 Ma and 1991+\-7 Ma (Hawke et al., 2014).||Unit of Bryah Group.||Overlain by Ravelstone Formation. Underlain by, and grades landward to Karalundi Formation.|Basalt, locally pillowed and plagioglase-phyric; mafic and ultramafic schist; locally pillowed, interbedded with volcaniclastic and siliciclastic sedimentary rocks.|30-AUG-19
13894|Narracoota Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bryah Basin.||Bryah Group, lower|||Basalt, locally pillowed and plagioclase-phyric, and mafic--ultramafic schist; interbedded with volcaniclastic and sedimentary rocks; metamorphosed.|
13940|Neale Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
13940|Neale Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
13940|Neale Formation|23314|5|Briefly described|331 Fig.2|||||||||
13940|Neale Formation|24390|5|Briefly described|p12 Table 3|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
13940|Neale Formation|41751|6|Mentioned|p8|||||||||
13940|Neale Formation|44111|6|Mentioned|p.58, Fig. 2|||in Officer Basin. Includes evaporites, stromatolitic carbonates and red beds.||||||
13940|Neale Formation|64793|6|Mentioned|p293|||Western Officer Basin. Hosts Baicalia burra Stromatolite Assemblage.||||||
13940|Neale Formation|65102|4|Described|p365, 366,367,372, Figs.4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin.10-500?m. Ilma & Neale Fms may correlate with Lefroy Fm or overlie it. Stromatolitic and oolitic dolomite, limestone; minor quartzite; shallow marine, part intertidal; base of unit not seen; type section at 28deg 15min S, 125deg 15min E; contains baicalia cf. burra.||||||
13940|Neale Formation|65366|5|Briefly described|p21|||Near Neale Junction, Northwestern Officer Basin||||||
13940|Neale Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin. Part of Supersequence 1.||||||
13940|Neale Formation|65416|6|Mentioned|p139 Fig.4, p140.|Neoproterozoic|Neoproterozoic|||||Overlies Browne Formation. Is unconformably overlain by Lennis Sandstone.||
13940|Neale Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, chert, quartzite, crystalline dolostone/dolomite|
13960|Neereno Sandstone|24160|6|Mentioned|p27 Tb. 14|Proterozoic|Proterozoic|||Billeranga Subgroup||||
13960|Neereno Sandstone|24410|5|Briefly described|p142 Tb. 60|||Of the Billeranga Subgroup (Moora Group). Unconformably over an Archaean basement.||||||24-NOV-09
13960|Neereno Sandstone|36293|6|Mentioned|p76|||Refers Arriens & Lalor 1959 and Low 1975.||||||
13960|Neereno Sandstone|36872|4|Described|p74|||||||||
13960|Neereno Sandstone|37460|6|Mentioned|p178|||||||||
13960|Neereno Sandstone|40307|6|Mentioned|p62|||||||||
13960|Neereno Sandstone|40347|6|Mentioned|p18|||||||||
13960|Neereno Sandstone|41957|6|Mentioned|p68|||||||||
13975|Nellie Tonalite|23722|4|Described|p12|Proterozoic|Proterozoic|Geological Province: Hooper Complex||||||
13975|Nellie Tonalite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
13975|Nellie Tonalite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13975|Nellie Tonalite|30897|5|Briefly described|p9|||||||||
13975|Nellie Tonalite|30898|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13975|Nellie Tonalite|36885|4|Described|p170|||||||||
13975|Nellie Tonalite|42814|5|Briefly described|p8|||||||||
13975|Nellie Tonalite|42815|5|Briefly described|map|||||||||
13975|Nellie Tonalite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
13975|Nellie Tonalite|44155|5|Briefly described|p239 Tb.3-3, p247|||||Hooper Complex.||Intrudes Halls Creek Group.|Hornblende-biotite tonalite, granodiorite; metamorphosed; locally strongly sheared.|
13975|Nellie Tonalite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
13975|Nellie Tonalite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Foliated medium grained hornblende biotite tonalite, diorite, and granodiorite, with minor pegmatite; chloritic schist and quartz veining associated with shears and along contacts|
13975|Nellie Tonalite|72437|5|Briefly described|p62|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated granodiorite.|
13990|Nelson Shale|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Geological Province: Ord Basin.||||||
13990|Nelson Shale|22547|4|Described|p30||Early Cambrian|Of the Negri Subgroup. Geological province: Ord Basin. Thickness: 180 m. Overlies Headley Limestone.||||||14-NOV-06
13990|Nelson Shale|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Of Negri Subgroup. Geological Province: Ord Basin. Max. thickness: 18 m.||||||
13990|Nelson Shale|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Goose Hole Group. Geological Province: Ord Basin.||||||
13990|Nelson Shale|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.  Maximum thickness: 180m.||||||
13990|Nelson Shale|28255|3|Fully described|p96|Cambrian|Cambrian|Grey and red, calcareous and gypsiferous shales and mudstone; minor limestone. Conformably overlies Headleys Limestone; conformably underlies Linnekar Limestone. Max. thickness: 165m. See also Table 9 (before p83) and p143 Appendix.||||||
13990|Nelson Shale|32172|4|Described|Table 2|||Middle Camb.||||||
13990|Nelson Shale|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Grey and red calcareous shales with gypsum bands and mudstone.  Conformably overlies Headleys Limestone; conformably overlain by the Linnekar Limestone.||||||20-NOV-06
13990|Nelson Shale|32648|6|Mentioned|p32|||M.Camb.||||||
13990|Nelson Shale|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
13990|Nelson Shale|36551|6|Mentioned|Table 16|||||||||
13990|Nelson Shale|36890|3|Fully described|p396|||||||||
13990|Nelson Shale|39210|5|Briefly described|Fig.18|||||||||
13990|Nelson Shale|40993|6|Mentioned|Fig.1|||||||||
13990|Nelson Shale|41840|2|Defined|p41|Middle Cambrian||||||||
13990|Nelson Shale|41864|3|Fully described|p18|||||||||
13990|Nelson Shale|41865|5|Briefly described|Map Legend|Middle Cambrian||||||||
13990|Nelson Shale|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
13990|Nelson Shale|42070|6|Mentioned|Fig.9 P12|||||||||
13990|Nelson Shale|43299|5|Briefly described|Map Legend||Cambrian|Of the Negri Subgroup.||||||20-NOV-06
13990|Nelson Shale|43853|5|Briefly described|Map Legend||Ordian|||||||
13990|Nelson Shale|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
13990|Nelson Shale|44317|4|Described|Table 4||Cambrian|||||||
13990|Nelson Shale|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian.||||||
13990|Nelson Shale|44363|5|Briefly described|p.6,18,20||Middle Cambrian|Middle Cambrian, Negri Group.||||||
13990|Nelson Shale|44364|14|Not recorded|map legend|||||||||
13990|Nelson Shale|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
13990|Nelson Shale|44965|14|Not recorded|Not recorded|||||||||
13990|Nelson Shale|45047|6|Mentioned|p126|||||||||
13990|Nelson Shale|48943|3|Fully described|p108|||Strat. table p139.||||||20-NOV-06
13990|Nelson Shale|60419|3|Fully described|p1, p3 Fig.2, p5|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Headleys Limestone. Conformably overlain by Linnekar Limestone. Max. thickness: 183 m. Maroon gypsiferous shale and mudstone. Geological Province: Ord Basin.||||||
13990|Nelson Shale|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Purple siltstone and mudstone; minor feldspathic sandstone. Geological Province: Ord Basin.||||||03-NOV-04
13990|Nelson Shale|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Maroon and grey gypsiferous shale and mudstone, minor sandstone, laminated limestone.  Conformably overlies Headleys Limestone; conformably overlain by the Linnekar Limestone. Geological Province: Ord Basin.||||||24-NOV-04
13990|Nelson Shale|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
13990|Nelson Shale|67860|4|Described|p417 Fig4-85, p420 Tb.4-18, p421 fig4-86|Middle Cambrian|Middle Cambrian|100-183 m thick. Type section details given. Contains rare Girvanella fossils.||Negri Subgroup||Conformably overlies Headleys Limestone or Antrim Plateau Volcanics. Is conformably overlain by Linnekar Limestone.|Purple gypsiferous siltstone and sandstone; minor micritic limestone.|
13990|Nelson Shale|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3|Series 3|Ord Basin||Negri Subgroup|||gypsiferous siltstone and mudstone; minor micritic limestone|
13990|Nelson Shale|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Gypsiferous siltstone and mudstone; minor micritic limestone.|
13990|Nelson Shale|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Headleys Limestone. Is overlain by Linnekar Limestone.||12-JUL-16
13990|Nelson Shale|69448|4|Described|p33:2-5, 8-9|Middle Cambrian|Middle Cambrian|Traves (1955). Ord Basin. 100-183m thick. Intertidal to supratidal deposits. Recessive unit: widely distributed but poorly exposed. Ordian age. Associated with uneconomic stratabound copper at contact with Headleys Limestone.||Negri Subgroup.||Conformably overlies Headleys Limestone or (locally) Antrim Plateau Volcanics unconformably. Is overlain conformably by Linnekar Limestone.|Maroon to grey, gypsiferous and pyritic shale and mudstone, minor fine sandstone, rare laminated limestone; unfossiliferous except for calcimicrobe Girvanella.|12-JUL-16
13990|Nelson Shale|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Gypsiferous siltstone and mudstone; minor micritic limestone|
13990|Nelson Shale|69673|5|Briefly described|p192, p193|Cambrian|Cambrian|183m thick.||Negri Subgroup||Overlain by Linnekar Limestone, overlies Headleys Limestone|Gypsiferous and pyritic shale and mudstone with minor sandstone and rare laminated limestone, deposited under peritidal conditions.|
13990|Nelson Shale|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Gypsiferous siltstone and mudstone; minor micritic limestone.|
13990|Nelson Shale|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|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.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Maroon and grey gypsiferous shale and mudstone, minor sandstone, laminated limestone.|
13990|Nelson Shale|71800|5|Briefly described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin.||Negri Subgroup||Overlies the Headleys Limestone. Overlain by the Linnekar Limestone.||
13990|Nelson Shale|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Headleys Limestone, underlies the Linnekar Limestone.||
14051|New Formation|41751|6|Mentioned|p4|||||||||
14108|Newmarracarra Limestone|22535|6|Mentioned|p493|||||||||
14108|Newmarracarra Limestone|23279|6|Mentioned|p28|||||||||
14108|Newmarracarra Limestone|23578|5|Briefly described|p7|Middle Jurassic|Middle Jurassic|Parent: Cadda Formation.||||||01-OCT-08
14108|Newmarracarra Limestone|23816|4|Described|p244, 245|Bajocian|Bajocian|Geological Province: Perth Basin. Of the Champion Bay Group. Underlying units: Colalura Sandstone and Bringo Shale (both conformable). Overlying unit: Kojarena Sandstone (conformable). Max. thickness: 11.5 m. Richly Fossiliferous.||||||27-APR-05
14108|Newmarracarra Limestone|24020|5|Briefly described|p387|Bajocian|Bajocian|Of Champion Bay Group. Geological Province: Perth Basin||||||16-MAR-05
14108|Newmarracarra Limestone|29548|6|Mentioned|p230|||M. Jurassic||||||
14108|Newmarracarra Limestone|30948|6|Mentioned|Map legend|Bajocian|Bajocian|||||||
14108|Newmarracarra Limestone|31561|5|Briefly described|p6|||See also P22. Bajocian||||||
14108|Newmarracarra Limestone|31562|6|Mentioned|p10|||Stratigraphic table||||||
14108|Newmarracarra Limestone|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
14108|Newmarracarra Limestone|31910|6|Mentioned|p22|||||||||
14108|Newmarracarra Limestone|32648|6|Mentioned|p32|||M.Jur. (in Champion Bay Gp.)||||||
14108|Newmarracarra Limestone|32649|4|Described|p25|||See also Table 1||||||
14108|Newmarracarra Limestone|33022|6|Mentioned|p259|||Palaeomagnetism P265||||||
14108|Newmarracarra Limestone|33166|6|Mentioned|p58|||Bivalve faunas||||||
14108|Newmarracarra Limestone|34134|6|Mentioned|Cor.Chart|||Bajocian.||||||
14108|Newmarracarra Limestone|34287|6|Mentioned|p168|||See also PP174, 177||||||
14108|Newmarracarra Limestone|35059|6|Mentioned|Table.19|||||||||
14108|Newmarracarra Limestone|35282|6|Mentioned|p31|||||||||
14108|Newmarracarra Limestone|36257|6|Mentioned|Table 2.1|||||||||
14108|Newmarracarra Limestone|36293|2|Defined|p151|Bajocian|Bajocian|||||||
14108|Newmarracarra Limestone|36890|3|Fully described|p244|||Formerly Newmarracarra Beds and Newmarracarra Series.||||||01-OCT-08
14108|Newmarracarra Limestone|37577|6|Mentioned|p75|||||||||
14108|Newmarracarra Limestone|41284|4|Described|p91|||||||||
14108|Newmarracarra Limestone|41625|5|Briefly described|p1|||||||||
14108|Newmarracarra Limestone|41729|5|Briefly described|p454|||||||||
14108|Newmarracarra Limestone|42211|6|Mentioned|p310|||||||||
14108|Newmarracarra Limestone|42473|6|Mentioned|p12|||||||||
14108|Newmarracarra Limestone|42477|5|Briefly described|p56|||||||||
14108|Newmarracarra Limestone|42823|6|Mentioned|p124|||||||||
14108|Newmarracarra Limestone|43495|6|Mentioned|16|||||||||
14108|Newmarracarra Limestone|43710|6|Mentioned|p6|||||||||
14108|Newmarracarra Limestone|43828|6|Mentioned|p207|||||||||
14108|Newmarracarra Limestone|44144|4|Described|p505 Tb.4-21, p515|Bajocian|Bajocian|Type Section: Round Hill 28o45'31''S 114o48'23''E. 14m thick shallow marine sediments with a significant ammonite fauna enabling interregional correlations.||Champion Bay Group||Overlies Bringo Shale or Colalura Sandstone (both conformably). Overlies Moonyoonooka Sandstone disconformably. Overlain by Kojarena Sandstone conformably.|Yellow-grey, sandy or clayey limestone, rarely grading into calcareous sandstone.|
14108|Newmarracarra Limestone|44237|14|Not recorded|p.201-202||Middle Jurassic|(M.Jurassic). See also p197,199,206,210.||||||
14108|Newmarracarra Limestone|48848|14|Not recorded|p.83,92,93,96-101|||||||||
14108|Newmarracarra Limestone|60376|6|Mentioned|p23.|||Cadda sequence offshore is the chronostratigraphic equlivalent of the Newmarracarra Limestone. Contains ammonoids.||||||07-FEB-11
14108|Newmarracarra Limestone|61811|4|Described|pp29-31, p65.|Middle Jurassic|Middle Jurassic|Fossiliferous; bivalves, gastropods, ammonoids, nautiloids, belemnites, brachiopoods, annelids, echinoids, bryozoa, foraminifera and ostracods. Type section is on Round Hill, 300 m south of the disused siding of Grant on the Geraldton-Mullewa line; further details in Appendix 1.||Unit in Champion Bay Group.||Overlies Bringo Shale. Is overlain by Kojarena Sandstone.|Bioclastic limestone, locally leached and replaced by iron oxide.|
14108|Newmarracarra Limestone|64635|5|Briefly described|p16|Middle Jurassic|Middle Jurassic|Fossiliferous.||Of the Champion Bay Group.|||Fossiliferous limestone.|
14108|Newmarracarra Limestone|68135|5|Briefly described|p52|Bajocian|Bajocian|Contains ammonite fossils.||Champion Bay Group|||Fossiliferous limestone.|14-SEP-17
14130|Nickol River Formation|22449|6|Mentioned|P25, Table3 P27||Archean|Age of dacite is 3023 Ma||||||07-NOV-08
14130|Nickol River Formation|22471|6|Mentioned|25|Archean|Archean|Geol province Pilbara||||||07-NOV-08
14130|Nickol River Formation|23484|4|Described|p10 table 2|Archean|Archean|Of Roebourne Group.  Maximum thickness: 500m.||||||07-NOV-08
14130|Nickol River Formation|23783|5|Briefly described|p37 Tb. 3|Archean|Archean|||||||07-NOV-08
14130|Nickol River Formation|23784|5|Briefly described|p10|Archean|Archean|Of Roebourne Group.||||||07-NOV-08
14130|Nickol River Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Roebourne Group.  Max. thickness: 500m.  Geological Province: Pilbara Craton.||||||07-NOV-08
14130|Nickol River Formation|23793|4|Described|p14|Archean|Archean|Of Roebourne Group. See also page 12 table 2||||||07-NOV-08
14130|Nickol River Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Roebourne Group. Geological Province: Pilbara Craton.||||||07-NOV-08
14130|Nickol River Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|of the Roebourne Group.  Age: 3.27-3.26Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
14130|Nickol River Formation|23936|4|Described|Tb.1|Archean|Archean|Age: 3.27-3.26 Ga. Geological Province: Pilbara Craton.Of the Roebourne Group. Overlain by Regal Formation. Underlain by Ruth Well Formation.||||||07-NOV-08
14130|Nickol River Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Roebourne Group. Maximum thickness: 500m.||||||07-NOV-08
14130|Nickol River Formation|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Roebourne Group. Geological Province: Pilbara Craton||||||07-NOV-08
14130|Nickol River Formation|24184|4|Described|p710, p711 Tb.1|Archean|Archean|Parent: Roebourne Group. Overlying Unit: Regal Formation. Underlying Unit: Ruth Well Formation. Geological Province: Pilbara Craton. Max Thickness: 100-500m. Age: ca. 3270-3250Ma||||||07-NOV-08
14130|Nickol River Formation|24541|3|Fully described|p11 Tb.2, p18, p20|Archean|Archean|Of the Roebourne Group. Overlain by the Regal Formation. Age: Quartz-serecite schist protolith <3269+/-2 Ma and rhyolite dated at 3251+/-6 Ma. Maximum Thickness: 500m.||||||07-NOV-08
14130|Nickol River Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Roebourne Group (Pilbara Supergroup).  Age: 3270-3250Ma.  Chert, banded iron-formation, carbonate and ferruginous clastic sedimentary rocks, quartzite, conglomerate, felsic volcanic and intrusive rocks.||||||07-NOV-08
14130|Nickol River Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Roebourne Group. Volcanogenic sediments, chert. Conformably overlies Ruth Well Formation. Age: ca 3270-3250Ma. Max.thickness: 500m. Coeval with intrusion of Karratha Granodiorite. Geological Province: Pilbara Craton. See also p40-41.||||||07-FEB-11
14130|Nickol River Formation|30766|6|Mentioned|Fig.1|||||||||
14130|Nickol River Formation|34829|6|Mentioned|p69|||||||||
14130|Nickol River Formation|37373|4|Described|p75|||||||||
14130|Nickol River Formation|41594|6|Mentioned|p43|||||||||
14130|Nickol River Formation|44477|2|Defined|p.27||Archean|SF/50-6.||||||07-NOV-08
14130|Nickol River Formation|44478|14|Not recorded|map legend||Archean|||||||07-NOV-08
14130|Nickol River Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Roebourne Group. Geological Province: Pilbara Craton. Age: c. 3270 Ma||||||07-NOV-08
14130|Nickol River Formation|50430|4|Described|p161||Archean|Dominantly sedimentary. Conformably overlies Ruth Well Formation. Of the Roebourne Group.||||||07-NOV-08
14130|Nickol River Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: <3.3GaGa.  Geological Province: Pilbara Craton.||||||07-NOV-08
14130|Nickol River Formation|63441|5|Briefly described|p5 Tb.1, p24|Archean|Archean|Of Roebourne Group (Pilbara Supergroup). Overlies Ruth Well Formation; unconformably overlain by Cleaverville Formation. Age: c.3.27-3.25Ga. In structural contact with Regal Formation (Regal Terrane). Geological province: West Pilbara Superterrane.||||||07-FEB-11
14130|Nickol River Formation|63518|5|Briefly described|p752, p753 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton. Its sedimentary rock units are tectonically in contact with the Cleaverville greenstone belt.||||||07-NOV-08
14130|Nickol River Formation|63538|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Roebourne Group. Underlain by Ruth Well Formation. Geological Province: Pilbara Craton.||||||19-APR-13
14130|Nickol River Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Roebourne Group. Chert, banded-iron formation, sedimentary carbonate rocks, ferruginous, siliclastic rocks; quartzose sandstone, conglomerate, and felsi volcanic and intrusive rocks; metamorphosed.||||||07-NOV-08
14130|Nickol River Formation|64580|4|Described|map legend||Paleoarchean|Of Roebourne Group. Chert, banded iron-formation, sedimentary carbonate rocks, ferruginous siliciclastic rocks, quartzose sandstone, conglomerate, felsic volcanic and intrusive rocks; metamorphosed.||||||09-DEC-08
14130|Nickol River Formation|67201|4|Described|p7, p11, p12 Tb.1, p14-17, see comments|Archean|Archean|In northwestern Pilbara Craton, Karratha Terrane, West Pilbara Superterrane. Previously included (along with Ruth Well Formation) in Roebourne Group. Type area described; outcrops almost continuously for > 100 km. Deformed by thrusts, shears and mesoscopic recumbent folds. Thickness > 150 m. Kiyokawa et al. (2002) referred to same formation as 'Lydia Mine complex' (informal name). Detrital zircon (3269+/-2 Ma, SHRIMP U-Pb, Nelson 1988) in schistose metasandstone. Hiatus between Ruth Well Formation and Nickol River Formation of at least 20 m.y., possibly > 50 m.y. suggests these Formations should not be assigned to same (Roebourne) Group. Direct dating of Ruth Well Formation is needed to resolve this. Is probably intruded by Dampier Granitic Complex. Regal Thrust Zone lies between overlying Regal Formation and underlying Nickol River Formation. Page location continued: p25-26, p37, p40-44, p69.|c. 3220 Ma; < 3250 Ma, see comments also|Roebourne Group||Overlies Ruth Well Formation (tectonic contact). Unconformably overlies Karratha Granodiorite. Is unconformably overlain by Fortescue Group. See comments|Basal (mylonitic) quartzite and black chert overlain by ferruginous chert and shale, banded-iron formation, with sedimentary carbonate rocks increasing up succession; metamorphosed. Includes tectonically attenuated pebbly sandstone.|24-NOV-16
14130|Nickol River Formation|67888|5|Briefly described|p50||||<3250 Ma||||Conglomerates and sandstones.|
14130|Nickol River Formation|68035|5|Briefly described|p289, 294, p290 Fig 5|Paleoarchean|Paleoarchean|Karratha Terrane, NW Pilbara. ?shallow-water clastic successions and thick volcanic piles, in passive margin settings. Spelt also Nikol River Formation p289 and Nickel River Formation on p294.|3250 - 3225 Ma|||||
14130|Nickol River 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.|c. 3270-3250 Ma|Unit of Roebourne Group.|||Chert, banded iron-formation, sedimentary carbonate rocks, ferruginous siliciclastic rocks, quartzose sandstone, conglomerate, felsic volcanic and intrusive rocks; metamorphosed|
14130|Nickol River Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p12-13, p20 Tb.2|||Pilbara Craton. West Pilbara Superterrane. Overlying Karratha Terrane. Comprises all of Nickol River Basin. Tectonically deformed slices of Nickol River Formation form Regal Thrust zone.|3250 Ma|Roebourne Group||Overlies Ruth Well Formation. Is overlain by Regal Formation.|Sedimentary rocks. Basal quartzite and chert are overlain by metamorphosed shale, BIF, and carbonate rocks.|
14130|Nickol River Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
14130|Nickol River Formation|70775|4|Described|iv, p6, p10, p12-p13, p16|Paleoarchean|Paleoarchean|Nickol River Basin. Originally part of the Roebourne Group. In areas where lower sections of the formation are well preserved it consists of either metaconglomerate or pebbly quartzite. Originally named by Williams (1968) who described it as a metamorphosed succession of shale, siltstone, sandstone, conglomerate, dolomite, chert and jaspilite with locally intercalated volcanic rocks. Lithology discussed in some detail. This unit is extensively deformed by recumbent folding and tectonic interleaving of various rock types. Hosts mesoarchean gold hosted in sandstone and conglomerate. See also p19-p20, p22-p24, p26-p27, p29-p32, p44 fig 27, p47, p72-p73, p81.|3280 Ma-3160 Ma|||Unconformably overlies the Roebourne Group and the Karratha Granodiorite. Overlain by (or faulted against) the Regal Formation. Equivalent to the Dixon Island Formation.|Chert, banded iron-formation, sedimentary carbonate rocks, ferruginous siliciclastic rocks, quartzose sandstone, conglomerate and felsic volcanic and intrusive rocks.|
14130|Nickol River Formation|70826|6|Mentioned|p8|Paleoarchean|Paleoarchean|Karratha Terrain, Pilbara Craton.||||Unconformably overlies Roebourne Group and Cleland Supersuite.||
14130|Nickol River Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Nickol River Basin.|||||Quartzose sandstone, conglomerate, breccia, carbonate rocks, chert, and banded-iron formation; local felsic volcanic and intrusive rocks; metamorphosed.|
14130|Nickol River Formation|72668|6|Mentioned|p4|||Karratha Terrane of the West Pilbara Superterrane.||Roebourne Group||Overlies the Ruth Well Formation.||
14160|Nine Mile Monzogranite|22534|4|Described|p12|||||||||
14160|Nine Mile Monzogranite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
14160|Nine Mile Monzogranite|41786|6|Mentioned|Table 2|||||||||
14160|Nine Mile Monzogranite|42697|5|Briefly described|map legend|||||||||
14160|Nine Mile Monzogranite|42892|5|Briefly described|p46|||||||||
14160|Nine Mile Monzogranite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
14160|Nine Mile Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
14160|Nine Mile Monzogranite|43496|6|Mentioned|13|||||||||
14160|Nine Mile Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmnm]   Coarse-grained, porphyritic, biotite-bearing monzogranite.||||||
14160|Nine Mile Monzogranite|65204|6|Mentioned|p17 Tbl.2.|Neoarchean||1-4mm grains; K-feldspar phenocrysts aligned to regional foliation.||||||
14160|Nine Mile Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Coarse-grained, porphyritic, biotite monzogranite; pentrative foliation moderate to weak, strongest at contacts with greenstones.||||||07-FEB-11
14160|Nine Mile Monzogranite|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Coarse-grained, porphyritic biotite monzogranite; penetrative foliation moderate to weak, strongest at contacts with greenstones; domal core to regional (D2) anticline.|06-AUG-15
14160|Nine Mile Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Coarse-grained, porphyritic biotite monzogranite; penetrative foliation moderate to weak, strongest at contacts with greenstones; domal core to regional (D2) anticline.|
14160|Nine Mile Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
14160|Nine Mile 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)||||Coarse-grained, porphyritic biotite monzogranite; penetrative foliation moderate to weak, strongest at contacts with greenstones; domal core to regional (D2) anticline|
14165|Ninety Seven Mile Formation|42710|5|Briefly described|map legend|Proterozoic||Variation on Ninety Seven Mile Beds.||||||
14165|Ninety Seven Mile Formation|42811|4|Described|p29-30|Neoproterozoic|Neoproterozoic|1700 m thick.||||Lateral equivalent to Elimberrie Formation based on possible glacigene sediments||17-OCT-12
14165|Ninety Seven Mile Formation|43281|5|Briefly described|Map legend||Proterozoic|||||||
14165|Ninety Seven Mile Formation|64580|4|Described|map legend||Neoproterozoic|White to grey quartzite, diamictite, phyllite and phyllitic sandstone; metamorphosed amygaloidal basalt, chlorite schist, epidotized quartzite; minor metamorphosed tuff, rhyolite.||||||09-DEC-08
14165|Ninety Seven Mile Formation|69099|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic||||||White to grey quartzite, diamictite, phyllite and phyllitic sandstone; metamorphosed amygaloidal basalt, chlorite schist, epidotized quartzite; minor metamorphosed tuff, rhyolite.|03-AUG-15
14165|Ninety Seven Mile Formation|69165|4|Described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||White to grey quartzite, diamictite, phyllite and phyllitic sandstone; metamorphosed amygdaloidal basalt, chlorite schist, epidotized quartzite; minor metamorphosed tuff, rhyolite.|
14165|Ninety Seven Mile Formation|69634|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic||||||White to grey quartzite, diamictite, phyllite and phyllitic sandstone; metamorphosed amygaloidal basalt, chlorite schist, epidotized quartzite; minor metamorphosed tuff, rhyolite|
14165|Ninety Seven Mile Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|neoproterozoic|Neoproterozoic||541-1000 Ma||||Sandstone, diamictite, siltstone, limestone, phyllite, quartzite, metabasalt, metatuff, and metarhyolite|
14165|Ninety Seven Mile Formation|71267|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Of Oscar Range Sub-basin. Louisa Basin, Centralian Superbasin. Events: 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.|1000-541 Ma (inferred)||||White to grey and partly epidotised quartzite, conglomeratic diamictite, phyllite and phyllitic siltstone, amygdaloidal basalt, chlorite schist, and minor meta-tuff and meta-rhyolite|
14165|Ninety Seven Mile Formation|72034|6|Mentioned|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Informally grouped with Elimberrie Formation. Oscar Range Sub-basin, Louisa Basin.||||||
14166|Ningbing Group|13194|4|Described|p382 fig 4-59, p399, p402 fig 4-66|Devonian|Devonian|171-1166m thick Famennian reef complex.|||Buttons Formation, Garimala Limestone, Wungabal Limestone, Kamilili Formation, Djilirri Limestone.|In part equivalent to Bonaparte Formation.  Overlies Cockatoo Group.||
14166|Ningbing Group|13234|6|Mentioned|p253,p260 Tb.1, |Famennian|Famennian|Lack porosity-enhancing stromatoporoids. Is similar to fractured algal boundstones of Nullara Formation in Canning Basin.||||||
14166|Ningbing Group|14228|5|Briefly described|p6 fig3|Devonian|Devonian|Southern Bonaparte Basin.||||Overlies Cockatoo Group. Overlain by Langfield Group.||05-OCT-16
14166|Ningbing Group|22814|5|Briefly described|fig2|Early Carboniferous|Late Devonian|||||||
14166|Ningbing Group|23377|6|Mentioned|p212 Fig.5|Carboniferous|Devonian|Of Vulcan Sub-basin.||||||28-MAY-08
14166|Ningbing Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|24503|5|Briefly described|Map legend|Devonian|Devonian|Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone. Geological Province: Bonaparte Basin.||||||11-APR-08
14166|Ningbing Group|24569|5|Briefly described|p248 Fig. 3|Late Devonian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
14166|Ningbing Group|40993|4|Described|p7|||Previously defined as Ningbing Limestone.||||||20-NOV-06
14166|Ningbing Group|41459|6|Mentioned|Fig.2|||||||||
14166|Ningbing Group|41532|6|Mentioned|p292|||||||||
14166|Ningbing Group|41731|5|Briefly described|p578|||See also p574.||||||20-NOV-06
14166|Ningbing Group|41864|4|Described|p85|||||||||
14166|Ningbing Group|41865|6|Mentioned|Map legend||Famennian|||||||
14166|Ningbing Group|41867|6|Mentioned|Map legend||Famennian|||||||
14166|Ningbing Group|42030|6|Mentioned|p748|||||||||
14166|Ningbing Group|42175|5|Briefly described|Fig.2 P200|||||||||
14166|Ningbing Group|42442|5|Briefly described|Fig.6 P9|||In WA and NT.||||||20-NOV-06
14166|Ningbing Group|43236|6|Mentioned|p14,Fig.13.||Late Devonian|||||||
14166|Ningbing Group|43661|6|Mentioned|Fig.3|||||||||
14166|Ningbing Group|50085|5|Briefly described|p2 Fig. 2, p3 Tb. 1||Devonian|Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|60006|5|Briefly described|Map Legend|||Geological Province: Bonaparte Basin. Unconformably overlain by Langfield Group.||||||
14166|Ningbing Group|60364|4|Described|p184|Famennian|Famennian|Equivalent to part of Buttons Formation. Geological Province: Bonaparte Basin.||||||
14166|Ningbing Group|61023|5|Briefly described|p2 Fig. 2|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin.||||||17-MAR-08
14166|Ningbing Group|61542|5|Briefly described|p277 Fig. 2|Famennian|Famennian|Overlain by Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
14166|Ningbing Group|64159|5|Briefly described|p93|Late Devonian|Late Devonian|Hosts minor dolomite-mineralisation within the limestone reef complex.||||||
14166|Ningbing Group|64580|4|Described|map legend||Late Devonian|Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone; includes DJILLIRI, WUNGABAL, and GARIMALA LIMESTONES, and KAMILILI and BUTTONS FORMATIONS.||||||09-DEC-08
14166|Ningbing Group|64694|6|Mentioned|p232, p234 Fig.2, p245 Fig.9|Late Devonian|Devonian||||Includes Wungabal and Garimala Limestones, and Buttons Formation.|Is overlain by Milligans Formation.||
14166|Ningbing Group|65331|6|Mentioned|cross-section only|||Shown only as subsurface on cross-section, in Devonian colour.||||||
14166|Ningbing Group|69099|4|Described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian||||Includes Djilliri, Wungabal,and Garimala Limestones, and Kamilili And Buttons Formations||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone.|03-AUG-15
14166|Ningbing Group|69165|4|Described|500k_geologyp08_lut.csv|Famennian|Frasnian||||Includes Djilliri Limestone, Wungabal Limestone, Garimala Limestone, Kamilili Formation, Buttons Formation||Undivided; limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone.|
14166|Ningbing Group|69452|4|Described|p36:4; 36:6 Fig.36.5; 36:7-13, 15|Late Devonian|Late Devonian|Mory and Beere (1988); equivalent to Buttons Beds-Ningbing Limestone interval of Veevers and Roberts (1968). Divided into 5 Formations in WA; only Buttons Formation is recognised in NT where the Group is entirely subsurface; the rest is undivided. Thickness varies: 171m to 1166m; 1024m onshore (NT). Carbonate rocks deposited as a reef complex, similar to those in the Canning Basin. Lateral equivalent in part of Bonaparte Formation.|||Djilirri, Wungabal, Garimala Limestones; Kamilili, Buttons Formations.|Overlies Cockatoo Group conformably or disconformably, and Antrim Plateau Volcanics disconformably. Is overlain by Langfield Group conformably or disconformably, or by Weaber Group disconformably.|Undivided: fine-grained and lesser medium-grained limestone and dolostone with authigenic quartz; overlain by bioclastic and mottled limestone containing algal bioherms and abundant bioclastic fragments.|12-JUL-16
14166|Ningbing Group|69634|5|Briefly described|500k_geologyp08_lut.csv||Late Devonian||||Includes Djilliri Limestone, Wungubal Limestone, Garimala Limestone, Kamilili Formation and Buttons Formation.|||
14166|Ningbing Group|69653|6|Mentioned|p10, 14|Late Devonian|Late Devonian|Petrel Sub-basin. Shallow-marine to non-marine settings.||||Overlies Cockatoo Group. Is overlain by Langfield Group.|Fine-grained clastic and carbonate sediments.|
14166|Ningbing Group|69673|5|Briefly described|p167, p169, p170, p175, p177|Famennian|Famennian|Conventional petroleum potential. Sealed by Langfield Group.|||Includes Djilirri Limestone, Kamilili Formation, Wungabal Limestone, Garimala Limestone, Buttons Formation|Overlain by Langfield Group, conformably (or disconformably) overlies Cockatoo Group, disconformably overlies Antrim Plateau Volcanics|Limestone and dolostone with authigenic quartz and fossil fragments. Bioclastic and mottled limestone.|
14166|Ningbing Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Devonian|Devonian|See also Regional geology: Fig.8, p8, p11, p13, p16. An equivalent unit in the Petrel Sub-basin includes the middle (Famennian) part of the Bonaparte Formation. Oil shows occur in onshore Bonaparte Basin. Hosts gas in Vienta 1.||||||12-JUL-16
14166|Ningbing Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Famennian|Famennian||359-372 Ma||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone|
14166|Ningbing Group|70206|5|Briefly described|cross-section only|||||||Unconformably overlain by Weaber Group.||
14166|Ningbing Group|70812|6|Mentioned|p30, p38|||||||||
14166|Ningbing Group|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Southern Bonaparte Basin.||||||
14166|Ningbing Group|70851|6|Mentioned|p17|||||||||
14166|Ningbing Group|71146|5|Briefly described|p6|Famennian|Frasnian|Bonaparte Basin.||||Overlies the Cockatoo Group. Overlain by the Buttons Formation.|Carbonates.|
14166|Ningbing Group|71267|4|Described|GEOL_LUT_CSV files|Famennian|Famennian|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). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|372.2-358.9 Ma (biostrat)||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale and sandstone.|
14166|Ningbing Group|72034|5|Briefly described|500k_interpgeop16_lut|Famennian|Famennian|Southern Bonaparte Basin.  Age from biostratigraphy.|||||Limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone.|
14193|Nita Formation|7433|6|Mentioned|p25 Fig.2, p28 Fig.5. |Ordovician|Ordovician|Canning Basin. Marine carbonates.||||||
14193|Nita Formation|13255|6|Mentioned|p368|Middle Ordovician|Middle Ordovician|Roebuck Basin.||||Overlies Goldwyer Formation. Is overlain by Carribuddy Group.||
14193|Nita Formation|13995|5|Briefly described|p67-68, p101|Ordovician|Ordovician|Canning Basin. Six of the twelve species of chitinozoans in this unit occur in coeval assemblages in Spitsbergen and Laurentia.||||Overlies Goldwyer Formation.|Shallow-water, regressive dolomite.|
14193|Nita Formation|14228|5|Briefly described|p6 fig3|Middle Ordovician|Middle Ordovician|Canning Basin.||||Overlies Goldwyer Formation. Overlain by Bongabinni Formation (Carribuddy Group).||06-OCT-16
14193|Nita Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Canning Basin.||||||
14193|Nita Formation|22738|4|Described|11,12,16, map|Ordovician|Ordovician|Max thickness 150 m. Overlain by Grant Group, Carribuddy Formation; underlain by Goldwyer Formation.||||||13-NOV-07
14193|Nita Formation|22741|6|Mentioned|P21|||||||||
14193|Nita Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
14193|Nita Formation|22764|6|Mentioned|p13|||||||||01-FEB-10
14193|Nita Formation|22765|5|Briefly described|P7, Table1||Llanvirn|||||||
14193|Nita Formation|22767|5|Briefly described|Table3 P18, P11||Ordovician|||||||
14193|Nita Formation|22776|4|Described|p10, Table.3|Ordovician|Ordovician|||||||
14193|Nita Formation|22801|5|Briefly described|P10, Table1 P9||Ordovician|||||||
14193|Nita Formation|22814|5|Briefly described|fig2|Ordovician|Early Ordovician|||||||
14193|Nita Formation|23212|4|Described|Table.1 p6||Ordovician|Age: Maximum age is late Middle Ordovician.||||||
14193|Nita Formation|24061|4|Described|p178|Middle Ordovician|Middle Ordovician|Geological Province:  Canning Basin. Maximum thickness: 259m.||||||
14193|Nita Formation|24246|5|Briefly described|p10, 11|Ordovician|Ordovician|Overlain by Caribuddy Formation. Geological Province: Canning Basin.||||||
14193|Nita Formation|24390|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
14193|Nita Formation|24449|5|Briefly described|p744, p741 Fig. 2|Llanvirnian|Llanvirnian|Geological Province: Canning Basin (Willara Sub-basin).  See also p473 Fig. 5.||||||
14193|Nita Formation|32648|6|Mentioned|p32|||U.Ord.||||||
14193|Nita Formation|33518|6|Mentioned|p4|||||||||
14193|Nita Formation|33738|6|Mentioned|p55|||||||||
14193|Nita Formation|33965|4|Described|Table 1|||||||||
14193|Nita Formation|35119|4|Described|p462|||Mention Text-Fig.3.||||||
14193|Nita Formation|35226|6|Mentioned|p9|||||||||
14193|Nita Formation|36224|5|Briefly described|Map legend|Ordovician|Ordovician|Dolomite, limestone, shale. Overlies the Goldwyer Formation.||||||19-JAN-10
14193|Nita Formation|36438|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14193|Nita Formation|36634|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14193|Nita Formation|36890|3|Fully described|p324|||||||||
14193|Nita Formation|37369|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14193|Nita Formation|37370|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14193|Nita Formation|38732|6|Mentioned|p33|||||||||
14193|Nita Formation|38878|6|Mentioned|Map legend|Llandeilian|Llanvirnian|Llandeilian - Llanvirnian||||||
14193|Nita Formation|39854|6|Mentioned|p21|||||||||
14193|Nita Formation|39857|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14193|Nita Formation|40078|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|Early to Middle OrdovicianE - M||||||
14193|Nita Formation|40136|5|Briefly described|p34|||||||||
14193|Nita Formation|40837|5|Briefly described|p258 and Fig. 5 insert|Middle Ordovician|Middle Ordovician|Overlain by Carribuddy Group.||||||25-FEB-08
14193|Nita Formation|40992|6|Mentioned|p17|||||||||
14193|Nita Formation|41169|6|Mentioned|p140|||||||||
14193|Nita Formation|41209|6|Mentioned|p143|||||||||
14193|Nita Formation|41215|6|Mentioned|p265|||See also P267 and P282||||||
14193|Nita Formation|41730|6|Mentioned|p471|||||||||
14193|Nita Formation|41854|4|Described|p95|||||||||
14193|Nita Formation|41913|6|Mentioned|Fig.2 P107|||||||||
14193|Nita Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
14193|Nita Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
14193|Nita Formation|42930|5|Briefly described|Fig.1 p473|Ordovician|Ordovician|Conformably overlies Goldwyer Formation. Geological Province: Canning Basin.||||||13-NOV-07
14193|Nita Formation|43173|6|Mentioned|11,54||Late Ordovician|||||||
14193|Nita Formation|43236|6|Mentioned|p14||Ordovician|Canning Basin||||||
14193|Nita Formation|43563|6|Mentioned|Fig.2,p5|||||||||
14193|Nita Formation|43599|6|Mentioned|p250, Fig.3||Llanvirnian|||||||
14193|Nita Formation|43656|6|Mentioned|Fig.2,p8|Llanvirnian|Llanvirnian|||||||
14193|Nita Formation|43666|6|Mentioned|p20||Llanvirnian|||||||
14193|Nita Formation|43746|6|Mentioned|Fig.2,p11|Llanvirnian|Llanvirnian|||||||
14193|Nita Formation|43803|6|Mentioned|p65||Ordovician|||||||
14193|Nita Formation|43815|6|Mentioned|Table 2,p95-96|||||||||
14193|Nita Formation|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
14193|Nita Formation|43825|5|Briefly described|p148|||||||||
14193|Nita Formation|44143|4|Described|p426, p428 Fig.4-94, p441 Table 4-19|Ordovician|Ordovician|Up to 240m thick; limestone, dolomite & shale; shallow marine. Conformably overlies Goldwyer Formation. Type section between 1165 and 1269m in Parda 1 (LAGRANGE: 18deg 56' 08" S, 122deg 00' 34" E). Contains conodonts & microflora; Llanvirian to Llandeilian. Has good petroleum-reservoir potential.||||||
14193|Nita Formation|44356|6|Mentioned|p8|Late Ordovician|Early Ordovician|(Middle-Late Ordovician)||||||
14193|Nita Formation|44357|5|Briefly described|p11,Tb.1 p10||Early Ordovician|(Middle Ordovician)||||||
14193|Nita Formation|45153|2|Defined|App.1-10|Middle Ordovician|Middle Ordovician|See also App.2-24.||||||13-NOV-07
14193|Nita Formation|45158|3|Fully described|p28|||||||||
14193|Nita Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
14193|Nita Formation|50028|6|Mentioned|p4|||Geological Province: Canning Basin.||||||
14193|Nita Formation|50085|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
14193|Nita Formation|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
14193|Nita Formation|50091|5|Briefly described|p413 Tb. 1|Late Ordovician|Late Ordovician|Occurrence of Panderodus nogamii (conodonts).  Geological Province: Canning Basin.||||||
14193|Nita Formation|50098|5|Briefly described|p4, p10|Ordovician|Ordovician|Geological Province: Canning Basin.||||||04-MAY-05
14193|Nita Formation|60119|5|Briefly described|p25|Ordovician|Ordovician|Rocks with oil-bearing potential.  Geological Province: Canning Basin.||||||22-JUL-04
14193|Nita Formation|61020|6|Mentioned|p33 Fig. 4|||Lead for petroleum potential.  Geological Province: Canning Basin.||||||20-APR-05
14193|Nita Formation|61021|5|Briefly described|p36 Fig. 2|Llanvirnian|Llanvirnian|Common hydrocarbon shows. Overlies the Goldwyer Formation; underlies the Carribuddy Group. Geological Province: Canning Basin.||||||17-DEC-07
14193|Nita 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
14193|Nita Formation|61551|5|Briefly described|p351 Fig.2, p359. |Darriwilian|Darriwilian|Canning Basin. Is a hydrocarbon reservoir in the sub-salt play in the Blina oil field.|||||Carbonates and clastics.|
14193|Nita Formation|62982|5|Briefly described|p7|Ordovician|Ordovician|Bioturbated carbonate and mudstone deposits; richly fossiliferous. Overlies Goldwyer  Formation. Geological Province: Canning Basin. The coarse vuggy dolomitised carbonates are potential reservoirs.||||||16-JAN-07
14193|Nita Formation|64185|5|Briefly described|p158 Fig. 2, p164, p165, p166-168|Late Ordovician|Early Ordovician|Underlain conformably by Goldwyer Formation. Max thickness: 225m.  Intertidal - shallow marine. See p164 for more detailed information.||||||
14193|Nita Formation|64186|4|Described|p169, p171-177, p173 Fig. 3, p170 Fig. 1|Late Ordovician|Ordovician|Underlain by Goldwyer Formation, overlain by Carribuddy Formation. Max thick: 130m. Geol Prov: Cannin Basin. Regressive and grades from limestone with shale beds at base to dolomite with argillaceous shale and limestone interbeds at top.||||||
14193|Nita Formation|64187|5|Briefly described|p320 Fig. 2|Silurian|Middle Ordovician|Formation is Fm in text. Underlain by Goldwyer Formation, overlain unconformably by Carribuddy Formation. Dolomite, limestone (marine). Geological Province: Canning Basin.||||||08-FEB-10
14193|Nita Formation|64334|5|Briefly described|p39-40, 42-43|Ordovician|Ordovician|Canning Basin; subsurface only. Llanvirn. Sub-economic oil surface flows.||||Overlies Goldwyer Formation. Is overlain by Bongabinni Formation (Carribuddy Group).|Dolostone. Fossiliferous.|
14193|Nita Formation|64513|6|Mentioned|p24, p31, p35.|Darriwilian|Darriwilian|Canning Basin. Mentioned in the text and p34 Fig.4 with respect to faunal zones.||||Overlies Goldwyer Formation.|Includes fossiliferous rock.|
14193|Nita Formation|64643|5|Briefly described|p3 Fig. 2|Darriwilian|Darriwilian|||||||
14193|Nita Formation|64975|5|Briefly described|pp162-163.|||||||Overlies Goldwyer Formation. Is overlain by Carribuddy Formation.|Carbonates.|
14193|Nita Formation|64982|4|Described|p695, p701, p703 Fig.8.|Ordovician|Ordovician|South Canning Basin. 1996 Looma 1 exploration well encountered low-permeability oil-bearing intervals. 50 - 110 m thick deposits in subtidal to supratidal environments. Article details the petrography. Sealed by Bongabinni Formation and Mallowa Salt.||||Overlies Goldwyer Formation.|Contains up to 43 progradational cycles of limestones, dolomites and shales.|
14193|Nita Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Ordovician|Middle Ordovician|Geological province: Canning Basin, Broome Platform. Includes dolomite. Commonly targeted as a potential reservoir. See also p8 Fig. 5.||||||
14193|Nita Formation|65449|3|Fully described|p1, p3, p5-10, p13, p17,p19, p34, p37-38|Darriwilian|Darriwilian|See also p47-50, p55; Plates 1-11. Named by McTavish and Legg (1972), but without a definition. Used by Williams that year in a well report for a carbonate unit between the Carribuddy and Goldwyer Formations. Formalised by Playford et al. (1975) who nominated the interval 1165-1270m in Parda 1 as the type section. Its two Members are defined in this Report. Fossiliferous marine unit, including Darriwilian conodonts; these correlate it with the lower part of Stokes Siltstone (Amadeus Basin). Potential reservoir for Bongabinni Formation oil. Oil was recovered from this unit in Leo 1; geochemical analysis indicated Bongabinni Formation source.|||Leo and Cudalgarra Members.|Overlies Goldwyer Formation. Is overlain conformably (locally unconformably) by Bongabinni Formation (Carribuddy Group).|Shallow cyclic carbonate and shale package; essentially free of coarse siliciclastics.|
14193|Nita Formation|68007|4|Described|p1-2, p4-5, p11-12, p14-15, Plates 1, 2|Middle Ordovician|Middle Ordovician|Canning Basin. Fossiliferous marine unit. Oil and gas shows. Carbonate-dominated; includes diagenetic dolomite. Targeted as potential reservoir. A possible equivalent occurs as a 43m-thick interval in Patience 2 well. Composite well log.||||Overlies Goldwyer Formation. Is conformably overlain by Carribuddy Group.|Light grey to grey-green and red-brown claystone and siltstone with minor argillaceous limestone and sandstone.|
14193|Nita Formation|68902|6|Mentioned|p9 fig 5|Ordovician|Ordovician|||||Overlies Goldwyer Formation, overlain by Bongabinni Formation.||
14193|Nita Formation|69029|6|Mentioned|p320|||Of Canning Basin.||||Overlain by the Carribuddy Group.||04-SEP-19
14193|Nita Formation|69182|5|Briefly described|Ch4 p9-p12, Ch4 p20-p25, Ch4 p30-p35|Upper Ordovician|Middle Ordovician|Canning Basin. Highly prospective reservoir unit for the storage of carbon dioxide with over 20 percent porosity and a permeability of 240 md. See also Ch4 p39-p41, Ch4 p44-p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p63, Ch4 p65, Ch4 p67, Ch4 p74, Ch4 p79-p82, Ch4 p92-p94.||||Overlies the Goldwyer Formation. Overlain by the Bongabinni Formation.|Dolomitic carbonates interbedded with claystones.|
14193|Nita Formation|69297|6|Mentioned|p350|Early Ordovician|Early Ordovician|Canning Basin. Deposited under marine or supratidal conditions.||||||
14193|Nita Formation|69312|5|Briefly described|p3, p7, p13 fig 13-14|Middle Ordovician|Middle Ordovician|Canning Basin. Petroleum reservoir rock that is sealed by the salts of the Carribuddy Group. See also p14 fig 15-16, p15, p19, p23 fig 26-27, p25 fig 30, p26 fig 32-33, p28 fig 36, p30.||||Overlies the Willara Formation. Overlain by the Bongabinni Formation.|Carbonate shales, marl.|11-FEB-20
14193|Nita Formation|69883|1|Redefined|p1-p6, p9-p14, p21-p22,|Llanvirn|Llanvirn|Canning Basin. Stratotype for this unit is the interval 1165-1270m in Parda 1. Deposited in a marine environment. Together with the Goldwyer Formation forms a transgressive-regressive package. Hydrocarbon shows are commonly reported most consistently within vuggy, dolomitized beds of this formation.  Intersected in at least 60 petroleum wells [see page 3 for names] and a number of mineral drillholes. The lower part is assigned to supersequence A2 and the upper part to supersequence B1. DD87SS7 is the stratotype for the members of this formation. Average thickness of 100m and reaches a maximum thickness of 216m in Crystal Creek 1. Conodonts form the basis for chronostratigraphy. See also p24, p31, p34, p36, p37-p38, p45, plate 1-4.|||Includes the Leo Member and the Cudalgarra Member.|Conformably overlies the Goldwyer Formation. Overlain by the Bongabinni Formation (Carribuddy Group). Unconformably overlain by the Poulton Formation.|Dolostone and limestone interbedded with lesser mudstone. Minor fine-grained sandstone also occurs.|02-MAR-20
14193|Nita Formation|70774|5|Briefly described|p4|Middle Ordovician|Middle Ordovician|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Goldwyer Formation. Overlain by the Bongabinni Formation (Carribuddy Group).||
14193|Nita Formation|71146|5|Briefly described|p6, p26|Middle Ordovician|Middle Ordovician|Canning Basin. Deposited in shallow, warm water environments. Together with the Goldwyer Formation hosts the giant Admiral Bay sulfide deposit.||||Overlies the Goldwyer Formation. Overlain by the Carribuddy Group.|Carbonates.|
14193|Nita Formation|71171|6|Mentioned|p2, p4|||Canning Basin.||||||
14193|Nita Formation|71870|5|Briefly described|p3, p5|Sandbian|Darriwilian|Canning Basin.||||Overlies the Goldwyer Formation. Overlain by the Bongabinni Formation (Carribuddy Group).||
14193|Nita Formation|71894|5|Briefly described|p4, p6|Middle Ordovician|Middle Ordovician|Canning Basin.||||Overlies the Goldwyer Formation. Overlain by the Bongabinni Formation.|Carbonate.|
14193|Nita Formation|72497|5|Briefly described|p3 Fig.2.|Middle Ordovician|Middle Ordovician|Shown, along with Goldwyer Formation, 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.||
14193|Nita Formation|72499|5|Briefly described|p7 Fig.6.|Middle Ordovician|Middle Ordovician|Located in the Willara Sub-basin and the Broome Platform.||||Overlies Goldwyer Formation and underlies Bongabinni Formation.|Includes carbonates.|
14193|Nita Formation|72500|5|Briefly described|p380-381, p389, p391-394, p396, p399|Darriwilian|Darriwilian|Canning Basin.||||Overlies the Goldwyer Formation.||28-AUG-20
14193|Nita Formation|72503|5|Briefly described|p25, p27-28, p30-32|||[Article discusses 2 conodonts from drill core section(s); neither are age-diagnostic].||||Conformably[?] underlain by Goldwyer Formation.|Includes dolostone, limestone, and mudstone.|
14193|Nita Formation|72504|6|Mentioned|Figure 3|||Canning Basin, Broome Platform. Intersected in Pictor 1,  Canopus 1, Looma 1, Robert 1, Fruitcake 1, Missing 1 and Sally May 2 drillholes.||||||18-MAR-20
14193|Nita Formation|73117|5|Briefly described|p3, p30, p141-142|Upper Ordovician|Middle Ordovician|Canning Basin.||||Underlain by Goldwyer Formation. Overlain by Bongabinni Formation (Carribuddy Group). Equivalent to Cobb Formation.|Dominantly carbonate.|
14193|Nita Formation|73344|6|Mentioned|p6, p42, Pl.1-3|Darriwilian|Darriwilian|Canning Basin, subsurface. Part of supersequence A2.||||Underlain by Goldwyer Formation. Overlain by Bongabinni Formation (Carribuddy Group).||
14193|Nita Formation|73346|6|Mentioned|p3, p27, App.1 p34|Middle Ordovician|Early Ordovician|Canning Basin. Deposited in shallow marine environments. May be age equivalent to Cobb Formation.||||||
14203|Noganyer Formation|22682|6|Mentioned|p12||Archean|Same as Penneshaw Formation. Also see Fig 9, p14||||||07-NOV-08
14203|Noganyer Formation|23136|6|Mentioned|p265 Fig.1|||||||||
14203|Noganyer Formation|23159|5|Briefly described|p790 fig4 table5|Archean|Archean|||||||07-NOV-08
14203|Noganyer Formation|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
14203|Noganyer Formation|23926|5|Briefly described|p9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
14203|Noganyer Formation|24165|5|Briefly described|p76|Archean|Archean|Iron King Mine, 5km SSE of Norseman. Mined for pyrite as a source of sulfur.|||Holstein Jaspilite, Iron King, Members.|||
14203|Noganyer Formation|30562|4|Described|p9|||See also P7: Archaean age||||||
14203|Noganyer Formation|30959|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
14203|Noganyer Formation|31093|6|Mentioned|Fig. 4|||||||||
14203|Noganyer Formation|36869|6|Mentioned|p48|||||||||
14203|Noganyer Formation|41432|5|Briefly described|p13|||||||||
14203|Noganyer Formation|42155|6|Mentioned|p369|||||||||
14203|Noganyer Formation|42195|5|Briefly described|p143|||See also Fig.2||||||
14203|Noganyer Formation|42221|4|Described|p32|||||||||
14203|Noganyer Formation|42626|6|Mentioned|Fig.4 P10|||||||||
14203|Noganyer Formation|42785|5|Briefly described|Fig.7 P275|||||||||
14203|Noganyer Formation|42937|5|Briefly described|p559|||||||||
14203|Noganyer Formation|43102|5|Briefly described|p11|||||||||
14203|Noganyer Formation|43162|6|Mentioned|6|||U-Pb age: 2714+/-5Ma||||||
14203|Noganyer Formation|43496|6|Mentioned|15|||Age: 2706+/-5Ma||||||
14203|Noganyer Formation|43498|5|Briefly described|2|||||||||
14203|Noganyer Formation|60076|4|Described|p15, p16 Fig. 6|Archean|Archean|Characterised by persistent BIF layers within clastic, partly felsic sedimentary rocks.  Overlies the Penneshaw Formation; overlain by Wolyeenyer Formation.  Within the Norseman greenstones region.||||||07-NOV-08
14203|Noganyer Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Norseman Terrane.  Kambalda Sequence.|||||Thinly-bedded turbidites and BIF.|
14203|Noganyer Formation|64633|6|Mentioned|p6 Fig.4.|||Kalgoorlie Terrane.|||||Sedimentary rocks, mainly fine-grained turbidites.|
14203|Noganyer Formation|65264|5|Briefly described|p11|||Overlain by Woolyeenyer Formation. Geological province: Norseman terrane. Characterised by laterally continuous BIF layers within clastic sedimentary rocks and intruded by sills. Overlain by Woolyeenyer Formation.||||||07-FEB-11
14203|Noganyer Formation|66880|5|Briefly described|pp7-8.|Archean|Archean|Norseman Terrane.|2684 +/- 5 Ma (Krapez et al. 2000).|||Is overlain by Woolyeenyer Formation.|Sedimentary rocks, mainly fine-grained turbidites.|
14203|Noganyer Formation|70326|4|Described|p360,364|Neoarchean|Neoarchean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Woolyeenyer Formation. Underlain by Pennshaw Formation.|Sedimentary rocks, banded iron formation, mafic and ultramafic rocks.|
14203|Noganyer Formation|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Kambalda Sequence||||
14203|Noganyer Formation|73391|5|Briefly described|p435-436, Appendices.|||Southern end of the Eastern Goldfields Province.|2864 +/- 5 Ma (Krapez et al., 2000).||||Epiclastic quartzose to quartzo-feldspathic sandstone-siltstone turbidites and carbonaceous shale, magnetic shale.|
14203|Noganyer Formation|73596|6|Mentioned|p1165, 1170|Mesoarchean|Mesoarchean|Norseman Inlier, Kalgoorlie-Kurnalpi Rift.|2864 +/- 5 Ma (MDA: Krapez et al., 2000).||||Sandstone.|
14208|Noingara Siltstone|24160|6|Mentioned|p26, p27 Tb.14|Proterozoic|Proterozoic|||Coomberdale Subgroup||Overlies Campbell Sandstone.||
14208|Noingara Siltstone|24410|5|Briefly described|p139|Proterozoic|Proterozoic|Of the Coomberdale Subgroup (Moora Group). See also p142 Tb. 60.||||||24-NOV-09
14208|Noingara Siltstone|34727|6|Mentioned|p68|||||||||
14208|Noingara Siltstone|36293|2|Defined|p68|Proterozoic|Proterozoic|||||||
14208|Noingara Siltstone|36872|3|Fully described|p77|||||||||
14208|Noingara Siltstone|37460|6|Mentioned|p178|||||||||
14208|Noingara Siltstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14208|Noingara Siltstone|40347|6|Mentioned|p20|||||||||
14208|Noingara Siltstone|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
14208|Noingara Siltstone|40349|5|Briefly described|p14|||||||||
14218|Noondine Chert|23279|6|Mentioned|p30||Proterozoic|||||||
14218|Noondine Chert|23761|5|Briefly described|p11|||Of the Moora Group.||||||25-OCT-05
14218|Noondine Chert|23762|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Moora Group.||||||
14218|Noondine Chert|24160|6|Mentioned|p26, p27 Tb.14|Proterozoic|Proterozoic|||Coomberdale Subgroup|||Silicified carbonate rock.|
14218|Noondine Chert|24410|5|Briefly described|p6, p139|Proterozoic|Proterozoic|Of the Coomberdale Subgroup. Silicified, bedded, carbonate unit; silicification of the chert is observed to a depth of 75m below surface. The chert is invariably hard to very hard.||||||24-NOV-09
14218|Noondine Chert|40307|6|Mentioned|p64|||||||||
14218|Noondine Chert|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14218|Noondine Chert|40347|6|Mentioned|p20|||||||||
14218|Noondine Chert|40348|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle or Late||||||
14218|Noondine Chert|40349|5|Briefly described|p14|||||||||
14218|Noondine Chert|42038|6|Mentioned|p108|||||||||
14218|Noondine Chert|44144|6|Mentioned|p511|||Rocks of this unit occur as glacial erratics in Nangetty Formation.|||||Stromatolitic chert.|
14242|Norcott Complex|37471|6|Mentioned|p1119|||||||||
14270|North Head Limestone|36890|4|Described|p356|||||||||
14270|North Head Limestone|44998|2|Defined|p.195,199||Cenozoic|||||||19-NOV-08
14270|North Head Limestone|45153|2|Defined|App.11-165|middle Holocene|middle Holocene|||||||
14270|North Head Limestone|64449|5|Briefly described|p62 Tb. 2, p63|Quaternary|Quaternary|Consists of bioclastic and quartzose fine clacarenite.||||||07-FEB-11
14271|North Kimberley kimberlite|41158|6|Mentioned|p250|||||||||
14281|North Star Basalt|23783|4|Described|p96|Archean|Archean|Of Talga Talga Subgroup.||||||07-NOV-08
14281|North Star Basalt|23807|6|Mentioned|p110 Fig. 2|||Geological Province: Pilbara Craton.||||||
14281|North Star 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
14281|North Star Basalt|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Talga Talga Subgroup. Massive basalt and pillow basalt. Max. Thickness: 2000m. Geological Province: Pilbara Craton.||||||07-NOV-08
14281|North Star Basalt|24184|5|Briefly described|p701, p699 Fig.3|Archean|Archean|Of the Talga Talga Subgroup. Overlain by McPhee Formation. Geological Province: Pilbara Craton. Age: ca.3490Ma (Ar-Ar, van Koolwijk et al, 2001).||||||07-NOV-08
14281|North Star Basalt|24185|5|Briefly described|p741 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
14281|North Star Basalt|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group).  Age: 3490Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
14281|North Star Basalt|24550|3|Fully described|p31 Tb. 3.1|Archean|Archean|Basal unit of Talga Talga Subgroup. Basalt is divided into informally named Units; Thin Chert, Clastic Seds, Middle Ultramafics, Upper Extrusives, Green Diorite Sills, Lower Ultramafics, Main Basalt; + the Big Chert forms the base of overlying McPhee Formation.||||||18-DEC-12
14281|North Star Basalt|24590|5|Briefly described|p29, p30 Fig. 1.3|Archean|Archean|Basal unit of the Talga Talga Subgroup (Warrawoona Group). Massive and pillow tholeiite, komatiite and chert. Overlain by McPhee Formation. Age: 3515Ma and 3560+/-32Ma. See also p84 Fig. 3.3, p193.||||||07-FEB-11
14281|North Star Basalt|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
14281|North Star Basalt|38498|5|Briefly described|Table 1|||||||||
14281|North Star Basalt|38510|6|Mentioned|p188|||||||||
14281|North Star Basalt|38544|6|Mentioned|Fig.1|||||||||
14281|North Star Basalt|39672|6|Mentioned|p240|||||||||
14281|North Star Basalt|39697|3|Fully described|p89|||||||||
14281|North Star Basalt|40596|6|Mentioned|p65|||||||||
14281|North Star Basalt|41028|6|Mentioned|p227|||||||||
14281|North Star Basalt|41029|5|Briefly described|p106|||||||||
14281|North Star Basalt|41636|6|Mentioned|p79|||||||||
14281|North Star Basalt|43595|6|Mentioned|Table 2-28,p214|||||||||
14281|North Star Basalt|43698|6|Mentioned|p18|||||||||
14281|North Star Basalt|43769|6|Mentioned|p858|||||||||
14281|North Star Basalt|44150|4|Described|p128, p129 Tb.2-15, p132 Fig.2-131|||See also p133 Tb.2-16, p137-140, p152 Tb.2-22, p157 Fig.2-144. Formerly part of Friendly Creek Formation (of Fitton et al., 1975) and part of Chocolate Hill Formation (Ingram, 1977).|3550 Ma.|Talga Talga Subgroup|||Metabasalt of greenschist to low amphibolite grade; local pillow lavas; metadolerite and metagabbro sills common.|
14281|North Star Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
14281|North Star Basalt|50381|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton. Age: 3490 Ma||||||09-APR-13
14281|North Star Basalt|50427|5|Briefly described|p192 Fig.11|Archean|Archean|Age: c.3316 Ma.||||||07-NOV-08
14281|North Star Basalt|60636|5|Briefly described|p34|Archean|Archean|Basal unit of the Warrawoona Group. Age: 3490Ma. See also p35-36 Fig. 3.2.||||||07-FEB-11
14281|North Star Basalt|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
14281|North Star Basalt|62427|5|Briefly described|p2, p3 Fig.2, p4, p17|Paleoarchean|Paleoarchean|Marble Bar Belt. Syndepositional activity of normal faults within the stratigraphic top of this unit.|3490 +/- 16 Ma.|Of the Warrawoona Group||||
14281|North Star Basalt|62979|5|Briefly described|p212 Fig. 1, p213 Fig. 2|Archean|Archean|Of the Warrawoona Group. Age: 3490Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
14281|North Star Basalt|63245|5|Briefly described|p5 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3515Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
14281|North Star Basalt|63420|5|Briefly described|Map legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup).  Age: c3490Ma. Geological Province: Pilbara Craton. Mafic volcanic rock; minor ultramafic rock and chert; metamorphosed.||||||07-NOV-08
14281|North Star Basalt|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup).||||||07-FEB-11
14281|North Star Basalt|63538|5|Briefly described|p8 Tb. 1, p8, p13, p6 Fig. 3|Archean|Archean|Of Warrawoona Group (Talga Talga Subgroup). Overlain by McPhee Formation. Geological Province: Pilbara Craton. Basalt.||||||19-APR-13
14281|North Star Basalt|64328|5|Briefly described|p56 Tb. 1|||Of Talga Talga Subgroup (Warrawoona Group). Basalt, ultramafic rock.||||||07-FEB-11
14281|North Star Basalt|64405|5|Briefly described|p4|Archean|Archean|Name inferred from North Star only in Figure 3. Of the Warrawoona Group (De Grey Supergroup).||||||07-FEB-11
14281|North Star Basalt|64621|5|Briefly described|Map legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group, Pilbara Supergroup). Age: <c.3490Ma. Lithology details for about 17 sub-units included.||||||07-NOV-08
14281|North Star Basalt|64747|6|Mentioned|p95 fig 2|Paleoarchean|Paleoarchean||3431 +/- 7 Ma (U-Pb zircon).|Unit in Warrawoona Group.||||
14281|North Star Basalt|64936|5|Briefly described|map legend|Archean|Archean|Of Talga Talga Subgroup. Under McPhee Formation. Under Corboy Formation. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
14281|North Star Basalt|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Talga Talga Subgroup. Mafic volcanic rocks, minor ultramafic rocks and chert; metamorphosed. Includes three mapped but unnamed units: grey, white and blue-black layered metachert; white and grey laminated recrystallised metachert; and amphibolite.||||||
14281|North Star Basalt|66217|4|Described|p5, pp14-16, p58.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Thickness to 2000 m. Age is an 40Ar/39Ar cooling age from hornblende from a retrogressed pyroxenite lens. Drill intersection in quartz veins in this unit at Myrnas Hill prospect show gold.|3490 +/- 15 Ma (van Koolwijk et al. 2001).|Basal unit in Talga Talga Subgroup.||Is intruded by Muccan and Mount Edgar Granitic Complexes. Is overlain conformably by McPhee and Dresser Formations.|Dominantly tholeiitic, massive and pillowed metabasalt, metakomatiitic basalt, serpentinised peridotite, and thin units of layered sedimentary chert including siliceous iron-formation; numerous sills of dolerite and gabbro.|
14281|North Star Basalt|66664|6|Mentioned|p4.  |||||||||
14281|North Star Basalt|66745|3|Fully described|p51, pp53-54, p56.|Paleoarchean|Paleoarchean|Basalts underlying Dresser Formation in the Panorama greenstone belt have been newly assigned to this unit. Thin ultramafic-mafic-chert cycles suggest either multiple heating events or a distal setting to more complete cycles developed elsewhere.|>3490 Ma.|Unit in Talga Talga Subgroup.||Is overlain by McPhee and Dresser Formations.|Basalt, komatiitic basalt, chert.|09-OCT-15
14281|North Star Basalt|67130|6|Mentioned|p15 fig 10|Paleoarchean|Paleoarchean||3480 Ma|Warrawoona Group||Overlain by Dresser Formation, McPhee Formation|Basalt and ultramafic lavas.|
14281|North Star Basalt|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3480 Ma.|Talga Talga Subgroup.||||
14281|North Star Basalt|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|> 3490 Ma|Talga Talga Subgroup||||
14281|North Star Basalt|67269|5|Briefly described|p5-6|Paleoarchean|Paleoarchean||>3490 Ma.|Warrawoona Group.||Is intruded by North Pole Monzogranite. Is overlain by Dresser Formation.|Basalt.|
14281|North Star Basalt|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|>3490 Ma.|Talga Talga Subgroup.||||
14281|North Star Basalt|67668|6|Mentioned|Fig. 2; p. 153||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group||Underlies the Dresser and McPhee Formations.|Mafic volcanic rocks.|
14281|North Star Basalt|68035|5|Briefly described|p288 Fig 4|Paleoarchean||Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.Thin ultramafic-mafic-chert cyles suggest either multiple heating events or a distal setting to more complete cyles developed elsewhere.|>3490 Ma|Of Talga Talga Subgroup.||Overlain by McPhee and Dresser Formations?|Basalt, komatiitic basalt, chert.|
14281|North Star Basalt|68280|5|Briefly described|p2, p4||||>3490 Ma|Talga Talga Subgroup||Overlain by McPhee Formation, Dresser Formation|Basalt, komatiitic basalt and chert.|17-JAN-23
14281|North Star Basalt|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age constrained by the parent Warrawoona Group.||Of the Warrawoona Group.||||02-DEC-14
14281|North Star Basalt|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Includes 2 unnamed subunits.|c.3490 Ma (Van Koolwijk et al. 2001).|Of the Talga Talga Subgroup.|||Metamorphosed mafic volcanic rock, minor ultramafic rock and chert; interlayered amphibolite and metamorphosed granitic rock, commonly schistose, includes granite and pegmatite veins; metamorphosed grey, white and blue-black layered chert.|23-SEP-13
14281|North Star Basalt|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3490 Ma.|Talga Talga Subgroup.||Is overlain by McPhee and/or Dresser Formations.||
14281|North Star Basalt|69012|5|Briefly described|Map Legend|Paleoarchean||East Pilbara Terrane. Six unnamed facies are mapped separately.|> 3490 Ma (van Koolwijk et al., 2001)|Of the Talga Talga Subgroup.|||Chert, basalt and dolerite, amphibolite and amphibolite schist, mafic volcanic rock, iron-formation with local quartz sandstone, komatiitic basalt: all metamorphosed.|28-APR-14
14281|North Star Basalt|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 5 unnamed sub-units.|>3490 Ma (van Koolwijk et al. 2001).|Of the Talga Talga Subgroup.|||Altered amphibolite and amphibolite schist; metabasalt and metadolerite; medium-grained, foliated amphibolite and amphibolite schist; carbonate-altered metabasalt; basalt (generally massive); includes syn-volcanic dolerite intrusions.|02-MAY-14
14281|North Star Basalt|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Mafic and ultramafic schist, serpentinized peridotite, serpentinite and serpentine-tremolite schist, layered chert; dolerite and gabbro; metamorphosed.||Talga Talga Subgroup|||komatiitic basalt and basalt, amphibolite and amphibolite schist intruded by granitic rocks. Metabasalt and metadolerite, carbonate altered metabasalt, silicified metakomatiitic basalt.|
14281|North Star Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1, p11, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane.|>3490 Ma|Talga Talga Subgroup|||Basalt, komatiitic basalt, chert.|
14281|North Star Basalt|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Warrawoona Group.||||
14281|North Star 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.|3515-3490 Ma (inferred)|Unit of Talga Talga Subgroup.|||Altered amphibolite and amphibolite schist; basalt; maddive, komatiitic, pillowed, metamorphosed; dolerite and gabbro dykes; layered chert and banded iron-formation; mafic and ultramafic schists; serpentinite and serpentinised peridotite.|
14281|North Star Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Talga Talga Subgroup.||||
14281|North Star Basalt|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.||Unit of Warrawoona Group.||||
14281|North Star Basalt|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|> 3490 Ma|Warrawoona Group||Overlies the Double Bar Formation. Overlain by the Dresser and McPhee Formations.||
14281|North Star Basalt|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.|3490 Ma.|||Is overlain by McPhee Formation.|Basalt, komatiite, some chert.|
14281|North Star Basalt|70884|5|Briefly described|p123-124|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|>3.49 Ga|Unit of Talga Talga Subgroup.||Overlain by Dresser Formation. Underlain by Double Bar Formation/Coonterunah Subgroup.||
14281|North Star Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|Max age ~3515 Ma, min 3490+/-15 Ma.|Talga Talga Subgroup|||Mafic volcanic rocks; minor ultramafic rocks and chert; metamorphosed.|
14281|North Star Basalt|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||Overlain by Dresser Formation. Underlain by Double Bar Formation.||
14281|North Star Basalt|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Talga Talga Subgroup.||Overlain by McPhee and Dresser formations. Underlain by Double Bar Formation.||
14281|North Star Basalt|72668|6|Mentioned|p4-6, p11|||East Pilbara Terrane.||Talga Talga Subgroup||Overlain by the McPhee and Dresser basalts.||
14281|North Star Basalt|73160|4|Described|p1-8, p9 Fig.7, p10-16|Paleoarchean|Paleoarchean|Pilbara Craton, East Pilbara Terrane. Majority of hydrothermal silica veins terminate immediately below or within the overlying North Pole Chert, vein network subdivided into discrete vein systems based on orientations and cross-cutting relationships. Zoned pattern of alteration assemblages, argillic adjacent to hydrothermal silica veins and progressively changing to phyllic then propylitic with increasing distance. Propylitic assemblage becomes progressively more actinolitic down-stratigraphy. Argillic zones and hydrothermal veins also widen upwards from the base of listric faults towards the paleo-surface. Upper part overprinted by low greenschist facies metamorphism. Illite Ar-Ar dating of three thermal events at 3249 Ma, 3061 Ma and 2294 Ma, postdating initial argillic alteration.  Also misspelt as North Pole Star Basalt p4.|~3490 Ma|Warrawoona Group||Conformably underlies Dresser Formation, North Pole Chert. Intruded by North Pole Monzogranite.|Pillow basalt, with hydrothermal alteration. Transected by a dense network of hydrothermal silica veins up to 20m wide. Hosts minor doleritic intrusions. Characterised by widespread kaolinisation alteration, most prevalent in upper parts.|
14281|North Star Basalt|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Talga Talga Subgroup.||Overlies North Star Formation. Is overlain by McPhee and Dresser Formations.||
14285|Northam gneiss|38789|6|Mentioned|Fig.2|||||||||
14333|Nuendah Formation|41199|2|Defined|p19|late Quaternary||Reserved as Nuendah||||||
14333|Nuendah Formation|50621|5|Briefly described|p159 Fig. 2|Cenozoic|Cenozoic|||||||19-NOV-08
14360|Nullara Limestone|22550|6|Mentioned|Fig 3|||||||||
14360|Nullara Limestone|22741|6|Mentioned|P22, Fig3||Devonian|||||||
14360|Nullara Limestone|22767|6|Mentioned|P20|||||||||
14360|Nullara Limestone|23338|5|Briefly described|915 Fig.3|Famennian|Frasnian|||||||
14360|Nullara Limestone|23722|4|Described|p31|Devonian|Devonian|Max. thickness: 400m. Geological Province: Canning Basin||||||28-MAY-08
14360|Nullara Limestone|23726|6|Mentioned|p43|||||||||
14360|Nullara Limestone|23903|5|Briefly described|p1597 Fig.2|Famennian|Famennian|Geological Province: Canning Basin||||||
14360|Nullara Limestone|24246|6|Mentioned|p10|Famennian|Famennian|Geological Province: Canning Basin.||||||
14360|Nullara Limestone|24377|6|Mentioned|P13|||Geological Province: Canning Basin||||||02-MAR-05
14360|Nullara Limestone|30181|6|Mentioned|p177|||See Definition card.||||||
14360|Nullara Limestone|31151|6|Mentioned|p68|||||||||
14360|Nullara Limestone|31152|6|Mentioned|Fig. 3|||||||||
14360|Nullara Limestone|32647|2|Defined|p98|Famennian|Famennian|Probably Famennian.||||||09-NOV-12
14360|Nullara Limestone|35104|6|Mentioned|p5|||||||||
14360|Nullara Limestone|36115|6|Mentioned|p133|||||||||
14360|Nullara Limestone|36365|6|Mentioned|p821|||||||||
14360|Nullara Limestone|38207|6|Mentioned|Fig.1|||||||||
14360|Nullara Limestone|39702|6|Mentioned|Fig.2|||||||||
14360|Nullara Limestone|40793|6|Mentioned|Fig.2|||||||||
14360|Nullara Limestone|40797|6|Mentioned|Fig.2|||||||||
14360|Nullara Limestone|40834|6|Mentioned|p140|||||||||
14360|Nullara Limestone|40837|6|Mentioned|Fig.5|||||||||
14360|Nullara Limestone|40838|6|Mentioned|p278|||||||||
14360|Nullara Limestone|40992|6|Mentioned|p17|||||||||
14360|Nullara Limestone|41023|6|Mentioned|p288|||||||||
14360|Nullara Limestone|41139|6|Mentioned|Fig.2|||||||||
14360|Nullara Limestone|41158|6|Mentioned|p80|||See also Plate 2||||||
14360|Nullara Limestone|41169|6|Mentioned|Fig.3|||||||||
14360|Nullara Limestone|41215|6|Mentioned|p278|||||||||
14360|Nullara Limestone|41217|5|Briefly described|Fig.2|||||||||
14360|Nullara Limestone|41839|6|Mentioned|p21|||||||||
14360|Nullara Limestone|41894|5|Briefly described|p4|||||||||
14360|Nullara Limestone|42030|5|Briefly described|p748|||||||||
14360|Nullara Limestone|42080|6|Mentioned|p281|||||||||
14360|Nullara Limestone|42111|6|Mentioned|Text fig.3 P90|||||||||
14360|Nullara Limestone|42191|6|Mentioned|p437|||||||||
14360|Nullara Limestone|42347|6|Mentioned|Fig.2 P1020|||||||||
14360|Nullara Limestone|42351|5|Briefly described|Fig.3 P40|||||||||
14360|Nullara Limestone|42564|5|Briefly described|Fig.5, 6 P6|||||||||
14360|Nullara Limestone|42710|5|Briefly described|map legend|Late Devonian||||||||
14360|Nullara Limestone|42811|4|Described|p42|||see also Fig.9.||||||13-NOV-07
14360|Nullara Limestone|42814|5|Briefly described|p23|||||||||
14360|Nullara Limestone|42815|5|Briefly described|map|Late Devonian||||||||
14360|Nullara Limestone|42860|5|Briefly described|Fig.2|||||||||
14360|Nullara Limestone|42880|5|Briefly described|Fig.2,p1020|||||||||
14360|Nullara Limestone|42930|5|Briefly described|Fig.1 p473|Early Carboniferous|Late Devonian|Conformably underlies Laurel Formation; partly overlies and interfingers with Windjana Limestone. Geological Province: Canning Basin.||||||13-NOV-07
14360|Nullara Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
14360|Nullara Limestone|43173|6|Mentioned|12-54||Late Devonian|||||||
14360|Nullara Limestone|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Canning Basin.||||||
14360|Nullara Limestone|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
14360|Nullara Limestone|43666|6|Mentioned|p23|||||||||
14360|Nullara Limestone|43723|6|Mentioned|p51||Devonian|||||||
14360|Nullara Limestone|44143|4|Described|p438 Table 4-19, p442, p443 Fig.4-98|Devonian|Devonian|Up to 300m thick; biostromal limestone, oolite & calcarenite; shallow marine. Interfingers with Windjana Limestone; is overlain conformably by Gumhole Formation. Type section 2km S of Mount Percy (LENNARD RIVER: 17deg 40' S, 124deg 56' 30" E). Contains conodonts and foraminifers; Famennian.||||||24-NOV-17
14360|Nullara Limestone|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Back-reef to reef-flat subfacies; massive cyanobacterial limestone; subordinate dolomite. Geological Province: Canning Basin.||||||19-MAY-05
14360|Nullara Limestone|45153|2|Defined|App.3-47|late Famennian|late Famennian|See also App.2-28.||||||13-NOV-07
14360|Nullara Limestone|45158|4|Described|p24|||||||||
14360|Nullara Limestone|46869|6|Mentioned|Fig.1|||||||||
14360|Nullara Limestone|46912|6|Mentioned|Table 1|||Analytical data of Canning Basin cores||||||
14360|Nullara Limestone|61551|6|Mentioned|p359, p361.|Upper Devonian|Upper Devonian|Canning Basin. Hydrocarbon (oil) source in the Blina field.||Unit in the Fairfield Group.||||
14360|Nullara Limestone|62575|5|Briefly described|p665|Famennian|Famennian|Limestone - back-reef facies. Geological Province: Canning Basin. Text refers to "the Famennian Nullara Sequence".||||||28-MAY-08
14360|Nullara Limestone|63110|6|Mentioned|p1135|||Age: 400Ma - 326Ma.||||||28-MAY-08
14360|Nullara Limestone|63938|5|Briefly described|p50 Fig.2|Famennian|Famennian|||||||
14360|Nullara Limestone|64159|5|Briefly described|p91 Fig. 6|Famennian|Famennian|Part of the Lennard Reef facies development.||||||
14360|Nullara Limestone|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Underlain by Windjana Limestone, overlain by Gumhole Formation. Limestone, dolomite (shallow marine). Geological Province: Canning Basin.||||||08-FEB-10
14360|Nullara Limestone|64502|5|Briefly described|p765 Fig. 2|Famennian|Famennian|||||||
14360|Nullara Limestone|64580|6|Mentioned|map legend|||Fammenian reef complexes, platform facies.||||||15-DEC-08
14360|Nullara Limestone|64643|5|Briefly described|p6, p7 Fig. 5, p35|||Back reef deposits.||||||
14360|Nullara Limestone|64981|5|Briefly described|p667, p672.|Famennian|Famennian|Lennard Shelf. Oil recovered from a highly fractured vuggy carbonate interval in this unit in 1981; sourced from Gogo Formation. Subsurface. Sealed by Fairfield Group shale.||||||
14360|Nullara Limestone|65301|6|Mentioned|p8 Fig. 5|||||||||
14360|Nullara Limestone|65486|5|Briefly described|p6-70, Plate 1.|Late Famennian|Middle Famennian|Reef, back-reef, and bank limestone, dolomite and sandstone, Canning Basin. Unconformably overlies Pillara Limestone. Overlies and interfingers with Windjana Limestone. Unconformably underlies Fairfield Group.||||||
14360|Nullara Limestone|66127|3|Fully described|pp19-21, pp48-49, pp168-174, pp329-332 |Famennian|Famennian|Of Playford and Cockbain (1976) for Famennian back-reef and bank subfacies of the platform facies; formerly Nullara Oolite of Smith et al. (1957). Named after Nullara Spring near the NE end of Oscar Range; type section is nearby, where it is 135 m thick. Mostly unfossiliferous. Has well-developed polygonal tepee structures. Hosts the productive Blina no. 1 oil well and others. Deposition cycles discussed in detail. No outcrop in Plates 5, 6 areas; shown in stratigraphic relationships diagram only. Shown on Plates 2, 3, 4, 5, 7, 8.||||Unconformably overlies Pillara Limestone; unconformably overlain by Fairfield and Grant Groups. Interfingers with Windjana Limestone and Piker Hills Formation.|Back-reef subfacies with well-bedded, fenestral, oolitic, and pelloidal limestone; locally dolomitized, sandy, and conglomeratic. Includes an unnamed unit of conglomerate, sandstone and siltstone in the Larrawa (Red Bluffs) area.|
14360|Nullara Limestone|66949|6|Mentioned|p28|Late Devonian|Late Devonian|Petroleum is produced from the top of this unit in the Blina field.||||||
14360|Nullara Limestone|67131|6|Mentioned|p1, p3 Fig. 2, p6-8, 10|Famennian|Famennian|Back-reef facies. Most complete outcrop section is in the Horseshoe Range; thin laminite-capped and tepee-pisolite-capped cycles occur at Barnett Spring (Napier Range).Equivalent to Nullara Sequences 1 + 2.||||Overlies Pillara Limestone. Overlain by Gumhole Formation.|Dolomitized, highly bioturbated crinoidal-peloidal packstones and grainstones; rare ooid grainstones.|03-FEB-20
14360|Nullara Limestone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Famennian|Famennian|Lennard Shelf. Canning Basin. Fammenian reef complexes, platform facies.|||||Well-bedded microbial, oolitic and peloidal limestone; locally dolomitized, sandy, or conglomeratic; Famennian back-reef platform facies in carbonate reef complexes.|03-AUG-15
14360|Nullara Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
14360|Nullara Limestone|69182|6|Mentioned|Ch4 p30-p35, Ch4 p39|||Canning Basin. Excellent reservoir potential for the storage of carbon dioxide. See also Ch4 p63, Ch4 p65, Ch4 p78.||||||
14360|Nullara Limestone|69297|6|Mentioned|p356|Upper Devonian|Upper Devonian|Canning Basin.||||||
14360|Nullara Limestone|69312|6|Mentioned|p9, p19|||Canning Basin. Reservoir of the Blina crude oil. See also p19, Nullara Formation p15, Nullara sequence p3, p23 Fig 27.||||Overlies the Pillara Limestone. Overlain by the Knobby Sandstone.|Sandstone.|11-FEB-20
14360|Nullara Limestone|69634|4|Described|GEOL_LUT_CSV files|Famennian|Famennian|Of Lennard Shelf, Canning Basin. Famennian back-reef platform facies in carbonate reef complexes. Events: Alice Springs Orogeny. See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|372.2-358.9 Ma (Biostrat)||||Well-bedded microbial, oolitic and peloidal limestone; locally dolomitized, sandy, or conglomeratic|
14360|Nullara Limestone|69660|5|Briefly described|Map legend|Famennian|Famennian|Canning Basin. Back-reef platform facies in carbonate reef complexes.|||||Well-bedded microbial, oolitic and peloidal limestone; locally dolomitized, sandy or conglomeratic.|
14360|Nullara Limestone|70154|4|Described|100k_interpgeop_lut.csv|Famennian|Famennian|See also 250k_interpgeop_lut.csv.|359-372 Ma||||Well bedded microbial, oolitic and peloidal limestone; locally dolomitized, sandy or conglomeratic. Famennian back-reef platform facies in carbonate reef complexes|
14360|Nullara Limestone|70272|6|Mentioned|p882|Famennian|Famennian|Lennard shelf, Canning Basin.||||||
14360|Nullara Limestone|71267|4|Described|GEOL_LUT_CSV files|Famennian|Famennian|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). Devonian reef complex. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|372.2-362 Ma (biostrat)||||Well-bedded microbial, oolitic and peloidal limestone; locally dolomitized, sandy, or conglomeratic; Famennian back-reef platform facies in carbonate reef complexes|
14360|Nullara Limestone|71892|6|Mentioned|p8, p10-p11, p27|Late Devonian|Late Devonian|Intruded by Ellendale diamondiferous pipe 4 (E4). Referred to as the Nullara Formation on p27, p29-30.|||||Limestone, sandstone and siltstone.|
14360|Nullara Limestone|72502|6|Mentioned|p3, p5|Famennian|Frasnian|Lennard Shelf, Canning Basin. Outcrops that underlie the Gumhole Formation at Horseshoe Range and Red Bluffs are birdseye limestone likely to constitute the uppermost facies of this unit.||||Probably overlain by Gumhole Formation. Underlain by Pillara Limestone. Equivalent to Windjana Limestone.|Birdseye limestone.|
14379|Nulsen Slate Member|30562|4|Described|p39|||Refers Hall & Bekker (1965). See also P37||||||
14379|Nulsen Slate Member|43162|6|Mentioned|6|||||||||
14385|Nummana Member|23047|5|Briefly described|40|||Of the Cheela Springs Basalt. Hamersley Province.  Max thickness 220 m.||||||10-FEB-09
14385|Nummana Member|23280|5|Briefly described|p1085-6,Fig2p1086|||||||||
14385|Nummana Member|35218|6|Mentioned|Fig.1|||||||||
14385|Nummana Member|35260|6|Mentioned|p17|||||||||
14385|Nummana Member|35976|6|Mentioned|Table 16|||||||||
14385|Nummana Member|36882|6|Mentioned|p135|||||||||
14385|Nummana Member|43595|5|Briefly described|Table 3-8,p344||Paleoproterozoic|||||||07-NOV-08
14385|Nummana Member|44692|4|Described|p.7,18,Tb.1, map|||O/lies Beasley River Quartzite. (F50-11).||||||
14385|Nummana Member|44729|5|Briefly described|map legend|Proterozoic||Of  Mount McGrath Formation.||||||
14385|Nummana Member|66574|5|Briefly described|p914 Fig.3, p914, p915, p917 Fig.5|||In lower Wyloo Group. Overlies Beasley River Quartzite; underlies Cheela Springs Basalt. Said to be a Member of Cheela Springs Basalt. Marine to fluvial siltstone, sandstone, plus basalt and dolerite sills.||||||
14385|Nummana Member|67130|5|Briefly described|p3 fig 2, p4, p25|||Misspelt as Numanna Member (p25)||Beasley River Quartzite||Conformably overlies Beasley River Quartzite, conformably overlain by Cheela Springs Basalt|Siltstone, sandstone and cross bedded quartz rich sandstone.|
14385|Nummana Member|68035|5|Briefly described|p292 fig 6|Paleoproterozoic|Paleoproterozoic|Wyloo Group, Ashburton Basin.||Of Beasley River Quartzite.||Overlain by Cheela Springs Basalt.|Sandstone, siltstone|
14385|Nummana Member|68280|5|Briefly described|p5, p51|||||Cheela Springs Basalt||Overlies Beasley River Quartzite|Cross bedded quartz sandstone and siltstone.|
14385|Nummana Member|69754|6|Mentioned|p317|||Pilbara Craton.||Beasley River Quartzite||||
14385|Nummana Member|70086|5|Briefly described|p196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Beasley River Quartzite.||Uppermost unit of the Beasley River Quartzite. Overlain by Cheela Springs Basalt.||
14385|Nummana Member|72712|5|Briefly described|p9, p30-31, p33, p41, p43, p36 Fig.25.|Rhyacian|Siderian|Previously considered part of Mount McGrath Formation (Halligan and Daniels, 1964), and the Beasley River Quartzite (Horwitz, 1978). Thickness varies from <50m to c. 300m in type section at Shingle Creek. Previously interpreted as a as a terrestrial red bed succession. A largely shallow marine to marginal marine interpretation is preferred here.|c. < 2276 Ma to c. 2250 Ma.|Basal Cheela Springs Basalt.||Overlies Beasley River Quartzite. Intruded by vesicular Balgara Dolerite.|Mainly interbedded mudstone and siltstone, with lesser conglomerate, fine to coarse-grained quartz arenite, amygdaloidal basalt flows, and dolerite sills with locally amygdaloidal tops.|
14404|Nunnery Sandstone|23815|4|Described|p282|Artinskian|Artinskian|Geological Province: Carnarvon Basin. Overlying unit: One Gum Formation (conformable). Underlying unit: Callytharra Formation (disconformable). Max. thickness: 166 m. Equivalent to the Moogooloo Sandstone.||||||
14404|Nunnery Sandstone|32648|6|Mentioned|p32|||In Wooramel Gp.||||||
14404|Nunnery Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
14404|Nunnery Sandstone|34532|6|Mentioned|p225|||Wooramel Gp.||||||
14404|Nunnery Sandstone|36890|3|Fully described|p282|||||||||
14404|Nunnery Sandstone|37295|6|Mentioned|Table 2|||||||||
14404|Nunnery Sandstone|41053|6|Mentioned|Fig.2|||||||||
14404|Nunnery Sandstone|42462|6|Mentioned|p55|||||||||
14404|Nunnery Sandstone|44217|14|Not recorded|Fig.3|||||||||
14404|Nunnery Sandstone|44532|4|Described|p.6, map|||(G50-5).||||||
14404|Nunnery Sandstone|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
14404|Nunnery Sandstone|44994|6|Mentioned|Fig.7|||Permian. Correlation.||||||
14404|Nunnery Sandstone|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
14404|Nunnery Sandstone|45016|2|Defined|p.108-115||Artinskian|Tb, p.58,69,74,75,77,87,90. (G50-6).||||||
14404|Nunnery Sandstone|48885|14|Not recorded|p.2,7,10,17,Pl.1||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6).||||||
14404|Nunnery Sandstone|60331|6|Mentioned|p33|||||||||
14404|Nunnery Sandstone|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
14404|Nunnery Sandstone|69547|6|Mentioned|p198|||Southern Carnarvon Basin.||||Underlain by Callytharra Formation.||
14404|Nunnery Sandstone|72910|6|Mentioned|p22.|Artinskian|Artinskian|Byro Sub-basin. Abandoned name, now believed to be, in part, equivalent to the Ballythanna Sandstone Member.|||||Includes sandstone.|
14410|Nura Nura Member|7433|5|Briefly described|pp34-35. |||Restricted to Fitzroy Sub-basin in Canning Basin. Braided-stream deposits passing laterally westward through deltaic, lagoonal and shallow-marine facies.||Lowermost unit in Poole Sandstone.||Overlies Carolyn Formation. Underlies Tuckfield Member.||
14410|Nura Nura Member|22718|6|Mentioned|P5|||||||||
14410|Nura Nura Member|22741|5|Briefly described|p27, Table3 p13||Sakmarian|||||||17-MAR-20
14410|Nura Nura Member|22753|5|Briefly described|Fig.3 p585|Permian|Permian|||||||
14410|Nura Nura Member|22765|6|Mentioned|P10|||||||||
14410|Nura Nura Member|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
14410|Nura Nura Member|22776|4|Described|Table.3|Early Permian|Early Permian|Of the Poole Sandstone, Age: Late Sakmarian. see also p19.||||||25-OCT-05
14410|Nura Nura Member|23523|5|Briefly described|p994 Fig. 2|Early Permian|Early Permian|||||||
14410|Nura Nura Member|23815|5|Briefly described|p281|Sakmarian|Sakmarian|Geological Province: Canning Basin. Of the Poole Sandstone.||||||27-APR-05
14410|Nura Nura Member|24466|5|Briefly described|p365|Early Permian|Early Permian|Of the Poole Sandstone. Overlain by the Tuckfield Member.||||||01-JUL-08
14410|Nura Nura Member|29548|6|Mentioned|p224|||L.Permian||||||
14410|Nura Nura Member|29817|5|Briefly described|p8|||||||||
14410|Nura Nura Member|29819|6|Mentioned|Map legend|Permian|Permian|||||||
14410|Nura Nura Member|30338|6|Mentioned|p101|||||||||
14410|Nura Nura Member|30342|3|Fully described|p103|||Member of Poole Sandstone. Sakmarian age.See also P104-106||||||
14410|Nura Nura Member|30545|6|Mentioned|p22|||Sakmarian. See also Fig.2||||||
14410|Nura Nura Member|31037|6|Mentioned|p1042|||Occurence of Metalogoceras striatem.||||||
14410|Nura Nura Member|32648|6|Mentioned|p32|||(Mb. of Poole Sandstone)||||||
14410|Nura Nura Member|32945|6|Mentioned|p73|||See also P88. Sakmarian||||||
14410|Nura Nura Member|33627|6|Mentioned|p582|||||||||
14410|Nura Nura Member|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
14410|Nura Nura Member|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
14410|Nura Nura Member|34287|6|Mentioned|p125|||Poole Sandstone||||||
14410|Nura Nura Member|34532|6|Mentioned|p220|||See also PP224-227||||||
14410|Nura Nura Member|35492|6|Mentioned|p145|||||||||
14410|Nura Nura Member|35983|6|Mentioned|Table 28|||||||||
14410|Nura Nura Member|36020|6|Mentioned|p387|||||||||
14410|Nura Nura Member|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Poole Sandstone.  Fine sandstone; mudstone, thin bedded, ripple marked, wavy and flaser bedding, bioturbated, fossiliferous.||||||01-FEB-05
14410|Nura Nura Member|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
14410|Nura Nura Member|36257|6|Mentioned|Table 2.1|||||||||
14410|Nura Nura Member|36596|6|Mentioned|Text Fig.5|||||||||
14410|Nura Nura Member|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
14410|Nura Nura Member|36890|3|Fully described|p340|||||||||
14410|Nura Nura Member|37106|5|Briefly described|p277|||||||||
14410|Nura Nura Member|37294|6|Mentioned|p104|||||||||
14410|Nura Nura Member|37549|6|Mentioned|p116|||||||||
14410|Nura Nura Member|38217|5|Briefly described|p269|||||||||
14410|Nura Nura Member|38586|6|Mentioned|p29|||||||||
14410|Nura Nura Member|38917|6|Mentioned|p169|||||||||
14410|Nura Nura Member|41044|6|Mentioned|p132|||||||||
14410|Nura Nura Member|41053|6|Mentioned|p98|||||||||
14410|Nura Nura Member|41100|6|Mentioned|Fig.8|||||||||
14410|Nura Nura Member|41169|6|Mentioned|Fig.3|||||||||
14410|Nura Nura Member|41315|6|Mentioned|p155|||||||||
14410|Nura Nura Member|41514|6|Mentioned|p68|||||||||
14410|Nura Nura Member|41730|6|Mentioned|p483|||||||||
14410|Nura Nura Member|42017|6|Mentioned|p1|||||||||
14410|Nura Nura Member|42540|6|Mentioned|p316|||Canning Basin||||||
14410|Nura Nura Member|42613|5|Briefly described|p14|||Of Poole Sandstone.||||||17-MAR-20
14410|Nura Nura Member|43015|5|Briefly described|Table 1,p319|||||||||
14410|Nura Nura Member|43018|6|Mentioned|p390|||Of Poole Sandstone.||||||01-JUL-08
14410|Nura Nura Member|43050|5|Briefly described|p16|||Of Poole Sandstone.||||||01-JUL-08
14410|Nura Nura Member|43173|6|Mentioned|54||Early Permian|||||||
14410|Nura Nura Member|43474|14|Not recorded|p71|||||||||
14410|Nura Nura Member|43563|6|Mentioned|Fig.2,p5|Artinskian|Sakmarian|||||||
14410|Nura Nura Member|43656|6|Mentioned|Fig.2,p8|Artinskian|Sakmarian|||||||
14410|Nura Nura Member|43666|6|Mentioned|p27||Sakmarian|||||||
14410|Nura Nura Member|43746|6|Mentioned|Fig.2,p11|Artinskian|Sakmarian|||||||
14410|Nura Nura Member|44219|14|Not recorded|p31,33||Sakmarian|pt. of Poole Sandstone.||||||
14410|Nura Nura Member|44479|2|Defined|opp.p.6, Tb.1|||E/51-1. Correlated with the Cuncudgerie Sandstone of this Sheet.||||||
14410|Nura Nura Member|44994|6|Mentioned|Fig.7|||Permian. Correlation||||||
14410|Nura Nura Member|44998|2|Defined|p.79||Artinskian|Base of Poole Sandstone. early Artinskian. On many pages. p.71,78,80,103-4. See also App.4 p288.||||||
14410|Nura Nura Member|45001|14|Not recorded|p7|Artinskian|Sakmarian|||||||
14410|Nura Nura Member|45016|14|Not recorded|p.62,72|||Tb. Correlated with Callytharra Formation.||||||
14410|Nura Nura Member|45031|14|Not recorded|p31|||Of Poole Sandstone.||||||
14410|Nura Nura Member|45158|4|Described|p20|||||||||
14410|Nura Nura Member|46849|6|Mentioned|p186|||||||||
14410|Nura Nura Member|48573|14|Not recorded|p.3,12,13.|||(E51-7/Alexander Creek)||||||
14410|Nura Nura Member|48596|14|Not recorded|p.5|||(E51-11)||||||
14410|Nura Nura Member|48831|14|Not recorded|p.22,54,57|||||||||
14410|Nura Nura Member|48848|14|Not recorded|p.86,90,96,101|||||||||
14410|Nura Nura Member|49644|5|Briefly described|Table|||||||||
14410|Nura Nura Member|60386|6|Mentioned|p297|Sakmarian|Sakmarian|Roebuck/Canning Basin. Deltaic - nearshore - shelf.||||||
14410|Nura Nura Member|61021|5|Briefly described|p36 Fig. 2|Artkinsian|Sakmarian|Geological Province: Canning Basin.||||||17-DEC-07
14410|Nura Nura Member|64186|6|Mentioned|p170 Fig. 1|Artinskian|Artinskian|Of Poole Sandstone.||||||
14410|Nura Nura Member|64630|5|Briefly described|p31 Fig.2|Sakmarian|Sakmarian|Province: Northern and Central Canning Basin.  A member of the Poole Sandstone, overlies the Grant Group. Palynology age: P. pseudoreticulata to S. fusus.||||||24-NOV-09
14410|Nura Nura Member|64643|5|Briefly described|p3 Fig. 2|Cisuralian|Cisuralian|Basal carbonate member of Poole Sandstone at Nura Nura Ridge. Sandy limestone with marine fossils.||||||
14410|Nura Nura Member|64971|5|Briefly described|p685 Fig. 2|Early Permian|Early Permian|||||||09-FEB-10
14410|Nura Nura Member|64974|5|Briefly described|p143, p148 Fig. 6|Late Sakmarian|Late Sakmarian|Of Poole Sandstone. Geological Province: Fitzroy Trough.||||||17-JUN-09
14410|Nura Nura Member|65301|5|Briefly described|p5 Fig. 4|Early Permian|Early Permian|Of Poole Sandstone. Geological province: Canning Basin.||||||
14410|Nura Nura Member|65449|6|Mentioned|p6|Cisuralian|Cisuralian|||Poole Sandstone.||||
14410|Nura Nura Member|66949|4|Described|p4 Fig.2;p11,p20-23;p48,50,52-53 Appx.2|Artinskian|Sakmarian|See also p57 Appx.3, p60-65 Appx.4; p68,71-73,75,77-80,83-84,86-91 Appx.5. Guppy et al. (1952); originally Nura-Nura Limestone of Wade (1937) [although Guppy et al. (1951) refer to the Nura Nura Limestone Member of Wade (1936)]. Type section detailed. Up to 20m thick; shallow marine deposits. Contains brachiopods, bivalves, bryozoans, forams, ostracods and ammonites. Appears below [?random error] Triassic heading on p57, but stated to be Sakmarian. Biostratigraphic zonation. Available core and Formation picks detailed.||Basal unit in Poole Sandstone.||Disconformably overlies Grant Group. Correlated with Fossil Cliff Member (Holmwood Shale) and Callytharra Formation.|Calcareous quartz sandstone and sandy limestone; fossiliferous limestone.|02-NOV-15
14410|Nura Nura Member|67354|5|Briefly described|p106.|||Canning Basin. Apparent correlative of marine beds in Ditji Formation, Bonaparte Basin. Contains conodont-bearing limestones.||Unit in Poole Sandstone.||||
14410|Nura Nura Member|68007|6|Mentioned|p4|Early Permian|Early Permian|Canning Basin.||||||25-FEB-20
14410|Nura Nura Member|68902|6|Mentioned|p9 fig 5|Permian|Permian|||Poole Sandstone||Unconformably overlies Grant Group.||
14410|Nura Nura Member|69182|6|Mentioned|Ch4 p15, Ch4 p87|Cisuralian|Cisuralian|Canning Basin.||Poole Sandstone||Overlies the Grant Group.|Carbonates.|
14410|Nura Nura Member|69297|6|Mentioned|p337, p352|Sakmarian|Sakmarian|Broome Platform of the Canning Basin.||Poole Sandstone||||
14410|Nura Nura Member|69547|4|Described|p180,182,188,190-191,199-200|Artinskian|Sakmarian|Canning Basin. Type section: Upper part of core 1 from 872.0m to 877.06m in the Perindi-1, Canning Basin, representing a marginal marine depositional environment. Overall stratigraphic thickness: 10-15m. Fossils (Metalegoceras clarkei Miller, Metalegoceras striatum Teichert, Thalassoceras wadei Miller and Propopanoceras ruzhencevi) recovered from the type area (locality 3 Fig 1; Canning Basin) indicate a Late Sakmarian age (Leonova, 1998, 2011; Boiko et al., 2008).||Unit of Poole Sandstone.||Basal unit of Poole Sandstone. Underlain by Grant Group.|Fossiliferous calcareous quartz sandstone and rare limestone interbedded with friable fine-grained sandstone.|
14410|Nura Nura Member|70774|4|Described|p4-p5, p7-p9|Artinskian|Sakmarian|Canning Basin. Previously the 'Nura Nura Limestone' of Wade (1936) before being renamed by Guppy et al., 1951. This has traditionally been defined as the basal unit of the Poole Sandstone (Guppy et al., 1958); more recent definitions specified a lenticular basal carbonate. Age derived from paleontological work (see p8). Distribution of facies and wireline characteristics are discussed. This unit is on average 8m thick with a maximum thickness of 13.5m and a minimum thickness of 2.5m. Interpreted to have been deposited in open widespread marine conditions as part of a shallow epicontintental sea. Petrographic descriptions are provided in appendix 3. See also p28-p30-p32, p37, p40-p41, p43, p49-p51, p57, p71, p75, p78-p82, p98-p100, p102-p104, Plate 1-Plate 6. Type section location given.||Poole Sandstone||Unconformably overlies the Clianthus Formation (Grant Group).|Limestone, fossiliferous sandstone and siltstone.|10-FEB-20
14410|Nura Nura Member|72497|5|Briefly described|p3 Fig.2, p12, p18.|Artinskian|Sakmarian|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. Includes shallow marine deposits.||Basal member of Poole Sandstone||Unconformably overlies upper Grant Group, Millajiddee Member.||
14410|Nura Nura Member|72499|4|Described|p8, 31, 38, 45, 46, 53,84,86,89,91,93,95|Artinskian|Artinskian|Recognised in Dampier Downs 1, Frome Rocks 2, Perindi 1, Roebuch Bay 1, Scarpia 1, Sundown 3.||Base of Poole Sandstone.|||Includes limestone and calcareous sandstone.|
14410|Nura Nura Member|72505|5|Briefly described|p890|Sakmarian|Sakmarian|Canning Basin. Correlates with the Presudo-reticulaspora pseudoreticulata zone.||Poole Sandstone||Unconformably overlies the Grant Group.||
14410|Nura Nura Member|73117|5|Briefly described|[See comments].|Asselian|Asselian|Canning Basin. Contains diverse macrofauna, foraminifera and rare conodonts of Sakmarian age. Includes distinctly marine, temperate-water facies. p: 14-15, 22, 25, 28-29, 39, 110-111, 113, 117, 120, 122, 124-131.||Poole Sandstone||Disconformably underlain by Grant Group.|Sandy carbonate-shale, marl.|
14424|Nyang Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Chararoo Supersuite.||||||07-FEB-11
14424|Nyang Granite|40909|6|Mentioned|p9|||||||||
14424|Nyang 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
14447|Nyuless Sandstone|22496|3|Fully described|p12||Neoproterozoic|Albert Edward Group, Wolfe Basin||||||
14447|Nyuless Sandstone|22547|6|Mentioned|p28||Neoproterozoic III|Of the Albert Edward Group.||||||14-NOV-06
14447|Nyuless Sandstone|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
14447|Nyuless Sandstone|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Overlying unit Flat Rock Formation. Underlying unit Timperley Shale. Geological Province: Wolfe Basin. Max. thickness: >10 m.||||||
14447|Nyuless Sandstone|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
14447|Nyuless Sandstone|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Albert Edward Group.||||||
14447|Nyuless Sandstone|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Albert Edward Group. Thin cap of lithic and quartz sandstone. Overlies Timperley Shale; overlain by Flat Rock Formation in Antrim and Ruby Plains. Geological Province: Wolfe Basin. Max Thickness: <10m.||||||06-APR-05
14447|Nyuless Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
14447|Nyuless Sandstone|32660|5|Briefly described|Table 6|||||||||
14447|Nyuless Sandstone|32728|6|Mentioned|Table 7|||See also Fig.16||||||
14447|Nyuless Sandstone|36551|6|Mentioned|Table 12|||||||||
14447|Nyuless Sandstone|36888|4|Described|p214|||||||||
14447|Nyuless Sandstone|36898|5|Briefly described|Table II|||||||||
14447|Nyuless Sandstone|37927|6|Mentioned|Fig.2|||||||||
14447|Nyuless Sandstone|38157|6|Mentioned|Table X|||||||||
14447|Nyuless Sandstone|41429|6|Mentioned|p248|||||||||
14447|Nyuless Sandstone|43299|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
14447|Nyuless Sandstone|43300|5|Briefly described|Map Legend||Neoproterozoic|||||||
14447|Nyuless Sandstone|43303|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
14447|Nyuless Sandstone|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 38 m thick.||Of Albert Edward Group.||Conformably overlies Timperley Shale. Overlain by Flat Rock Formation conformably.|Quartz sandstone, feldspathic sandstone, minor pebble conglomerate.|08-MAR-18
14447|Nyuless Sandstone|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean).||||||
14447|Nyuless Sandstone|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
14447|Nyuless Sandstone|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
14447|Nyuless Sandstone|45047|2|Defined|p97|Adelaidean|Adelaidean|Described p36.||||||28-MAY-15
14447|Nyuless Sandstone|45140|3|Fully described|p59, Appx.p38-39|||Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Nyuless Creek. [No type section details]. About 35m thick. No fossils known. NB: The definition in Appx.p39 has confused the overlying and underlying units.||Albert Edward Group.||Conformably overlies Timperley Shale. Is overlain conformably by Flat Rock Formation. See Comments.|Fine- to medium-grained quartz-rich arenite.|
14447|Nyuless Sandstone|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
14447|Nyuless Sandstone|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Albert Edward Group. Geological Province: Wolfe Creek Basin. Quartz sandstone and lithic sandstone; minor siltstone and conglomerate.||||||
14447|Nyuless Sandstone|63458|6|Mentioned|p873 Fig.2, p886 Fig.11, p897 Fig.19. |Ediacaran|Ediacaran|Appears as Nyuless Fm in Fig.11.||Unit in Albert Edward Group.||||
14447|Nyuless Sandstone|64104|6|Mentioned|p62 fig.1, p71 Tb. 2, p72 Fig.8|Neoproterozoic|Neoproterozoic|Appears as Nyuless Formation in Tb.2.||Albert Edward Group||Is overlain by Flat Rock Formation.||
14447|Nyuless Sandstone|67484|6|Mentioned|p294, p295 Fig.2|Ediacaran|Ediacaran|East Kimberley.||Of the Albert Edward Group.||Overlain by the Flat Rock Formation. Underlain by the Timperley Shale.||
14447|Nyuless Sandstone|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Timperley Shale. Is overlain by Flat Rock Formation.||
14447|Nyuless Sandstone|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Albert Edward Group.||||
14447|Nyuless Sandstone|68244|4|Described|p660|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region.||Unit of Albert Edward Group.||Overlain by Flat Rock Formation. Underlain by Timperley Shale.||
14447|Nyuless Sandstone|68473|6|Mentioned|p531, p533|||||Albert Edward Group||||
14447|Nyuless Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Of Albert Edward Group.|||quartz sandstone and lithic sandstone; minor siltstone and conglomerate|18-MAY-15
14447|Nyuless Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Quartz sandstone and lithic sandstone; minor siltstone and conglomerate.|
14447|Nyuless 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.|||Quartz sandstone and lithic sandstone; minor siltstone and conglomerate|
14447|Nyuless Sandstone|70154|6|Mentioned|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group||||
14447|Nyuless 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, 1m_geologyl12_lithology_lut.csv, 1m_geologyl12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Quartz sandstone and lithic sandstone; minor siltstone and conglomerate|
14447|Nyuless Sandstone|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||Albert Edward Group||Overlies the Timperley Shale, underlies the Flat Rock Sandstone.||
14452|O'Donnell Formation|22547|4|Described|p21||Orosirian|Of the Speewah Group. Geological province: Speewah Basin. Thickness: 260 m. Overlies Whitewater Volcanics. Overlain by Tunganary Formation.||||||14-NOV-06
14452|O'Donnell Formation|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
14452|O'Donnell Formation|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Speewah Group.||||||
14452|O'Donnell Formation|23751|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1834+/-3 Ma. Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 250 m.||||||07-NOV-08
14452|O'Donnell Formation|30097|6|Mentioned|Table 23|||Also Tables 24,28||||||
14452|O'Donnell Formation|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14452|O'Donnell Formation|30533|4|Described|p15|||ON Table 2||||||
14452|O'Donnell Formation|30558|6|Mentioned|p36|||||||||
14452|O'Donnell Formation|30894|5|Briefly described|p250|||Carpentarian||||||
14452|O'Donnell Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14452|O'Donnell Formation|30896|4|Described|p16|||||||||
14452|O'Donnell Formation|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14452|O'Donnell Formation|32660|5|Briefly described|Table 3|||||||||
14452|O'Donnell Formation|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
14452|O'Donnell Formation|32728|5|Briefly described|p34|||||||||
14452|O'Donnell Formation|36551|6|Mentioned|Table 10|||||||||
14452|O'Donnell Formation|36885|4|Described|p186|||||||||
14452|O'Donnell Formation|36902|6|Mentioned|p11|||||||||
14452|O'Donnell Formation|37462|6|Mentioned|Fig.4.9|||||||||
14452|O'Donnell Formation|38482|6|Mentioned|Table 1|||||||||
14452|O'Donnell Formation|41241|5|Briefly described|p132|||||||||
14452|O'Donnell Formation|41557|6|Mentioned|p598|||||||||
14452|O'Donnell Formation|41575|6|Mentioned|p592|||||||||
14452|O'Donnell Formation|41987|5|Briefly described|Fig.4 P74|||||||||
14452|O'Donnell Formation|42149|6|Mentioned|Table 1 P709|||||||||
14452|O'Donnell Formation|42710|5|Briefly described|map legend|Proterozoic||||||||
14452|O'Donnell Formation|42811|4|Described|p20|||of Speewah Group||||||
14452|O'Donnell Formation|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
14452|O'Donnell Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
14452|O'Donnell Formation|43854|5|Briefly described|Map Legend||Proterozoic|of Speewah Group.||||||
14452|O'Donnell Formation|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
14452|O'Donnell Formation|44140|5|Briefly described|p295, p297|Paleoproterozoic|Paleoproterozoic|30-523m thick. Two distinct members; marked lateral variations.||Speewah Group||Overlies Whitewater Volcanics. Is overlain by Luman Siltstone. Faulted over the Hooper Complex.|Quartz sandstone, granule sandstone, quartz greywacke, green shale and siltstone.|08-MAR-18
14452|O'Donnell Formation|44155|6|Mentioned|p242 Tb.3-5|||||Speewah Group||Overlies Little Gold River Porphyry unconformably.||
14452|O'Donnell Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
14452|O'Donnell Formation|44231|5|Briefly described|Map Legend||Proterozoic|Of the Speewah Group. Olive-green to fawn micaceous silty shale; coarse-grained quartz sandstone; granule to pebble conglomerate at base. Age: c.1835Ma. Geological Province: Canning Basin.||||||19-MAY-05
14452|O'Donnell Formation|44317|4|Described|Table 2||Carpentarian|||||||
14452|O'Donnell Formation|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
14452|O'Donnell Formation|44363|5|Briefly described|p.6,11,12|||(Carpentarian) Speewah Group.||||||
14452|O'Donnell Formation|44364|14|Not recorded|map legend|||||||||
14452|O'Donnell Formation|44366|14|Not recorded|p.11, Table 2||Carpentarian|Part of Speewah Group.||||||
14452|O'Donnell Formation|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Speewah Group.||||||
14452|O'Donnell Formation|44397|14|Not recorded|p.17, Table 2||Carpentarian|Speewah Group.||||||
14452|O'Donnell Formation|44398|14|Not recorded|map legend||Carpentarian|||||||
14452|O'Donnell Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
14452|O'Donnell Formation|45047|5|Briefly described|p28|||||||||
14452|O'Donnell Formation|48931|3|Fully described|p45|||||||||
14452|O'Donnell Formation|60714|6|Mentioned|p113 Fig.2. |||||Basal unit of Speewah Group.||Unconformably overlies Hooper and Lamboo Complexes. Is overlain by Tunganary Formation.||
14452|O'Donnell Formation|60724|6|Mentioned|p16, p17|||||||||
14452|O'Donnell Formation|64748|5|Briefly described|p269 Fig 2|||Of the Speewah Group; Underlies the Tunganary Formation; unconformably overlies the Hooper and Lamboo Complexes||||||
14452|O'Donnell Formation|67563|5|Briefly described|p121, p122 Fig.2|Orosirian|Orosirian|Youngest detrital zircon population age by Kirkland et al. (2010) who also gave another age of 1864 +/- 4 Ma.|1841 +/- 17 Ma|Of the Speewah Group.||||20-JAN-17
14452|O'Donnell Formation|68078|6|Mentioned|p5-6, p11, p14 figure 10, p23|Paleoproterozoic|Paleoproterozoic|Age is maximum depositional age.|1864 Ma +/- 4 Ma (SHRIMP)|Speewah Group||Overlain by Tunganary Formation||13-SEP-22
14452|O'Donnell Formation|68992|5|Briefly described|p498 Fig.1, p499||Orosirian|Speewah Basin. Youngest detrital zircon age.|1864 +/- 4 Ma (Kirkland et al, 2010a).|Of the Speewah Group.||||
14452|O'Donnell Formation|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|U-Pb zircon maximum depositional age.|<1864 Ma.|Speewah Group.||Is overlain by Tunganary Formation.||
14452|O'Donnell Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Min depositional age 1834+/-3 Ma (felsic volcanics in Valentine Siltstone, higher in Speewah Group). SHRIMP age from analyses released in 2010. See geochron file 182107.1.pdf for age, unit relations. Rb/Sr age: 1695 Ma|Max.deposit 1841+/-17 Ma U/Pb SHRIMP|Base of Speewah Group||Unconformably overlies Hooper Complex and western Lamboo Complex.|Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate|21-JUL-15
14452|O'Donnell Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1695 Ma|Speewah Group|||Fine to coarse grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, granule to pebble conglomerate.|
14452|O'Donnell Formation|69585|4|Described|p4-5, p7-12|Orosirian|Orosirian|Western Lamboo Province. High-energy fluvial, probably braided, river system. U-Pb and Lu-Hf zircon analytical data tabulated.|1864 +/- 4 Ma (maximum depositional age).|Basal Speewah Group.||Unconformably overlies Whitewater Volcanics and Paperbark Supersuite. Is overlain conformably by Tunganary Formation.|An overall fining-upward succession of poorly-sorted, coarse-grained, quartz-rich sandstone, lithic sandstone, pebbly sandstone, granule to pebble conglomerate, and chloritic siltstone and claystone.|
14452|O'Donnell Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Speewah Basin. Interpreted to have been deposited between 1834+\-3 Ma (age of a felsic volcanic unit in the Valentine Siltstone (Griffin et al., 1993) and after 1865-1850 Ma (age of crystalline rocks of the underlying Hooper Complex). 207Pb*/206Pb* date of 1841+\-17 Ma provides an interpreted maximum depositonal age (weighted mean 207Pb*/206Pb* date of 1864+\-4 Ma). Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1850-1835 Ma (Inferred)|Unit of Speewah Group.||Lowermost unit of Speewah Group. Underlain unconformably by Hooper Complex, Lamboo Complex.|Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate|
14452|O'Donnell Formation|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.||Unit in Speewah Group.|||Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate.|
14452|O'Donnell Formation|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.||Speewah Group.||Is overlain by Tunganary Formation.|Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate.|
14452|O'Donnell Formation|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1797-1835 Ma|Speewah Group|||Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate.|
14452|O'Donnell Formation|70812|5|Briefly described|p6|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1850-1800 Ma|Speewah Group||||
14452|O'Donnell Formation|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1850-1800 Ma|Speewah Group||Overlain by the Valentine Sandstone.|Sedimentary rocks.|24-MAR-23
14452|O'Donnell Formation|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.||Lowermost unit of Speewah Group. Overlain conformably by Tunganary Formation. Underlain unconformably by Hooper Complex, Lamboo Complex.|Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate|
14452|O'Donnell Formation|71281|4|Described|p421-422|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Speewah Basin. Up to 260m thick.||Basal Speewah Group.||Unconformably overlies Whitewater Volcanics and Paperbark Supersuite granites. Is overlain by Tunganary Formation.|Rippled and graded, massive, poorly sorted, coarse to granule quartz sandstone, locally lithic, ferruginous or glauconitic; olive green to fawn, micaceous silty shale; and conglomerate mainly near the base.|
14452|O'Donnell Formation|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.|||Fine- to coarse-grained quartz sandstone and lithic quartz sandstone, pebbly sandstone, chloritic siltstone and mudstone, and granule to pebble conglomerate.|
14452|O'Donnell Formation|72437|6|Mentioned|p12|Palaeoproterozoic|Palaeoproterozoic|Occurs on the DIXON RANGE map sheet where it is intruded by a dacite porphyry sill (equivalent to the rhyolite porphyry of Dow and Gemuts, 1967) which may be related to the volcanics in the Valentine Siltstone.||||||
14452|O'Donnell Formation|72490|5|Briefly described|p3|||Maximum thickness of 260 m.||Speewah Group|||Rippled and graded massive poorly sorted coarse to granule quartz sandstone, locally lithic, ferruginous or glauconitic; olive green to fawn micaceous silty shale, and conglomerate mainly near the base.|
14474|Oakover Formation|22717|5|Briefly described|P13||Tertiary|||||||
14474|Oakover Formation|23583|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
14474|Oakover Formation|23585|4|Described|p25|Cenozoic|Cenozoic|Max. thickness: 50 m.||||||19-NOV-08
14474|Oakover Formation|23594|4|Described|p24|||Geological Province: Canning Basin.||||||
14474|Oakover Formation|23745|5|Briefly described|p20|||See also page 3.||||||
14474|Oakover Formation|23746|4|Described|p29|||||||||
14474|Oakover Formation|24025|5|Briefly described|p16|Cenozoic|Cenozoic|Geological Province: Canning Basin.||||||19-NOV-08
14474|Oakover Formation|24573|6|Mentioned|p672 Fig.3|||Geological Province: Pilbara Craton||||||
14474|Oakover Formation|29770|6|Mentioned|p77|||||||||
14474|Oakover Formation|29845|6|Mentioned|Plate 3|||||||||
14474|Oakover Formation|30096|6|Mentioned|p75|||Refers to Lishmund (1967) search for diamonds.||||||
14474|Oakover Formation|30402|4|Described|Table 2|||||||||
14474|Oakover Formation|32972|5|Briefly described|p66|||Refers Mabbutt et al. (1963) Correlation.||||||
14474|Oakover Formation|33544|6|Mentioned|p25|||||||||
14474|Oakover Formation|34135|5|Briefly described|Table 1|||Tertiary. See also pp19,20||||||17-SEP-18
14474|Oakover Formation|35260|6|Mentioned|p19|||||||||
14474|Oakover Formation|35641|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14474|Oakover Formation|37564|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14474|Oakover Formation|37643|5|Briefly described|p5.5.3|||||||||
14474|Oakover Formation|39424|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14474|Oakover Formation|39426|4|Described|p15|||||||||
14474|Oakover Formation|39444|6|Mentioned|p46|||||||||
14474|Oakover Formation|39697|6|Mentioned|p138|||||||||
14474|Oakover Formation|40369|6|Mentioned|p17|||See also Plate 2||||||
14474|Oakover Formation|41669|3|Fully described|p51|||||||||
14474|Oakover Formation|41751|6|Mentioned|p8|||||||||
14474|Oakover Formation|43055|4|Described|p30|||||||||
14474|Oakover Formation|43056|5|Briefly described|Map Legend|||||||||
14474|Oakover Formation|43818|6|Mentioned|Fig.2.p39||Cenozoic|||||||19-NOV-08
14474|Oakover Formation|44143|4|Described|p429 Table 4-19, p451-452|Cainozoic|Cainozoic|Up to 30m thick; calcareous sandstone; lacustrine. Unconformably overlies Paterson Formation. Type locality is Oakover River valley. Contains ostracods.||||||24-NOV-17
14474|Oakover Formation|44189|5|Briefly described|Map legend||Cenozoic|||||||19-NOV-08
14474|Oakover Formation|44190|5|Briefly described|Map Legend||Cenozoic|||||||19-NOV-08
14474|Oakover Formation|44297|14|Not recorded|p.4,5,15,19,22|||(F51-9).||||||
14474|Oakover Formation|44298|14|Not recorded|map legend||Tertiary|||||||
14474|Oakover Formation|44438|14|Not recorded|map legend||Tertiary|||||||
14474|Oakover Formation|44443|5|Briefly described|map legend|Tertiary|Tertiary|||||||
14474|Oakover Formation|44477|6|Mentioned|p.16|||SF/50-6.||||||
14474|Oakover Formation|44478|14|Not recorded|map legend||Tertiary|||||||
14474|Oakover Formation|44501|14|Not recorded|p.22|||(F/50-8,F/51-5).||||||
14474|Oakover Formation|44503|2|Defined|p.8,18,Tb.2, map|||Roy Hill Sheet. (F50-12).||||||
14474|Oakover Formation|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
14474|Oakover Formation|44692|4|Described|p.7,8,20,21,Tb.1,map|||(F50-11).||||||
14474|Oakover Formation|44729|5|Briefly described|map legend|Tertiary|Tertiary|||||||
14474|Oakover Formation|44831|5|Briefly described|Map Legend||Cenozoic|||||||19-NOV-08
14474|Oakover Formation|45923|14|Not recorded|p.70||Tertiary|Map F51-5. Late?Tertiary.||||||
14474|Oakover Formation|46319|4|Described|p18|Cenozoic|Cenozoic|Maximum thickness: 30m.||||||19-NOV-08
14474|Oakover Formation|50287|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Limestone and calcareous sandstone.||||||19-NOV-08
14474|Oakover Formation|50544|4|Described|p66, p16 Tb. 1|Pliocene|Pliocene|Lacustrine carbonate deposits.  Age: 5-2Ma.  Max. thickness: upper unit of 8m and lower unit of 40m.||||||07-DEC-06
14474|Oakover Formation|50555|5|Briefly described|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
14474|Oakover Formation|60539|5|Briefly described|p500, 501 Fig.3|Miocene|Miocene|Overlies: Marillana Formation, specifically Iowa Eastern Member. Calcrete deposits.||||||
14474|Oakover Formation|63417|5|Briefly described|Map legend|Neogene|Paleogene|Undivided variously silicified limestone, silty limestone, calcareous sandstone, siltstone and marl.||||||
14474|Oakover Formation|63432|5|Briefly described| p736 Fig. 3, p752|||Overlies Marillana Formation. Calcrete/silcrete.||||||07-FEB-11
14474|Oakover Formation|64621|5|Briefly described|Map legend|Neogene|Neogene|Upper unit; vuggy, white to pale grey opaline silica, silicated carbonate and minor calcareous sandstone; lacustrine.||||||
14474|Oakover Formation|64656|5|Briefly described|Map Legend|Neogene|Neogene|Calcareous sandstone, siltstone, silty limestone, and marl; laucustrine deposit.||||||
14474|Oakover Formation|65194|6|Mentioned|p15, p101, p108, p112|Quaternary|Miocene|Calcareous lacustrine deposit. Pilbara area.||||||
14474|Oakover Formation|65724|5|Briefly described|map legend|Neogene|Paleogene|Upper unit: vuggy opaline silica, silicified carbonate rock, minor calcareous sand, lacustrine deposit; lower unit: limestone and calcareous sandstone, packstone, lacustrine deposit.||||||
14474|Oakover Formation|65825|5|Briefly described|p24.|Cenozoic|Cenozoic|Thought to be a lacustrine deposit. Regolith unit forming residual deposits on low hills and plateau remnants.|||||Limestone and calcareous sandstone.|
14474|Oakover Formation|65828|5|Briefly described|Map legend|Cenozoic|Cenozoic||||||Limestone and calcareous sandstone.|
14474|Oakover Formation|65829|3|Fully described|p6, p10, p29, pp31-33. |Neogene|Neogene|Lacustrine deposits. Outcrops as scattered buttes, mesas and dissected small tablelands. Pliocene. Upper siliceous unit, 3 to 10 m thick, is only found above the lower carbonate unit, up to 45 m thick. Resembles carbonates of Lawford and Nadarra Formations.|c.5 - 2 Ma.|||Overlies Paterson Formation, Pinjian Chert Breccia, Carawine Dolomite and Jeerinah Formation.|Widespread lower unit of limestone, calcareous sandstone and packstone, intertonguing with colluvium from adjacent bedrock; overlain by upper unit of vuggy, opaline silica, silicified carbonate rock and minor calcareous sandstone.|
14474|Oakover Formation|67183|5|Briefly described|p643 Fig.3, p648, p659 Fig.18 |Pleistocene|Pleistocene|Williams 1989||||Is unconformably underlain by Paterson Formation.|Flaggy limestone, carbonate, sandstone.|
14474|Oakover Formation|67202|5|Briefly described|p70,p73-74,p81,p120,p150, p257-258, p281|Neogene|Paleogene|Oakover River valley. Up to 50m thick. Forms mesas and plateaux of partly silicified calcrete after lacustrine limestone Deposited in a lacustrine environment.||||Overlies Paterson Formation.|A lower carbonate-rich unit and an upper chalcedonic unit. White vuggy opaline silica and chalcedony overprinting calcareous sandstone and limestone.|15-FEB-18
14474|Oakover Formation|69167|4|Described|geologyp_lut.csv|Neogene|Neogene||||||Variably silicified limestone, silty limestone, calcareous sandstone, siltstone, and marl.Limestone and calcareous sandstone; includes packstone. Vuggy opaline silica, silicified carbonate; lacustrine.|
14474|Oakover Formation|69538|5|Briefly described|p522 Fig.5, p527, p532 Tb.3, p534|Quaternary|Miocene|See also p559-561, p572-573, p576. Oakover Sub-basin in NE Pilbara. Overlies the CzD2 channel iron deposits. precise age uncertain but presumed to be similar to Millstream Formation which has Miocene to Pleistocene-Holocene gastropods.|||||Limestone (calcrete-silcrete).|17-SEP-18
14474|Oakover Formation|69590|4|Described|100k_geologyp_lut.csv|Neogene|Neogene|Of Canning Basin.|23-2.59 Ma (inferred)||||Variably silicified limestone, silty limestone, calcareous sandstone, siltstone, and marl; buggy, white to grey opaline silica, silicified carbonate.|
14474|Oakover Formation|71042|6|Mentioned|p69, p76, p79, p86|Cenozoic|Permian|Age between Permian Paterson Formation and Cenozoic gravels.|||||Flaggy limestone.|28-MAY-19
14474|Oakover Formation|71808|4|Described|p63-p65, p117|||Canning Basin. Equivalent rocks to this formation are exposed in the southwestern part of the survey area. Climate during deposition is discussed. Clasts in conglomerate are derived from Fortescue Group volcanics.|||||White micritic carbonate limestone/mudstone, conglomerate and red beds|
14474|Oakover Formation|73574|5|Briefly described|p762, p770|Quaternary|Miocene|Pilbara Craton.|||||Lacustrine carbonate deposits; limestone and calcareous sandstone; includes undivided variously silicified limestone, silty limestone, calcareous sandstone, siltstone and marl.|
14517|Old Leopold Hill lamproite|41158|6|Mentioned|p151|||||||||
14517|Old Leopold Hill lamproite|41828|6|Mentioned|p507|||||||||
14525|Older Granite|38514|5|Briefly described|Table II|||||||||
14547|Olia Gneiss|22716|5|Briefly described|table4, p237|Mesoproterozoic|Mesoproterozoic|Age: 1600 Ma.||||||
14547|Olia Gneiss|22826|4|Described|p567|Neoproterozoic|Neoproterozoic|The Olia Gneiss forms the basement to the Amadeus Basin in the south together with the Musgrave-Mann Complex. It is intruded by Granite and by dolerite dykes; overlain unconformably by the Dean Quartzite.||||||03-AUG-09
14547|Olia Gneiss|23483|5|Briefly described|p4|||||||||
14547|Olia Gneiss|23818|6|Mentioned|p43|||||||||
14547|Olia Gneiss|24197|5|Briefly described|p97|||Amphibolite-facies gneisses north of Woodroffe Thrust (Mulga Park Domain). Geological Province: Musgrave Block.||||||07-FEB-11
14547|Olia Gneiss|24496|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|May be protolith for some Pottyu Suite granitoids. Geological Province: Musgrave Block.||||||10-JUL-13
14547|Olia Gneiss|24499|5|Briefly described|Map legend|||||||||
14547|Olia Gneiss|30815|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
14547|Olia Gneiss|30817|5|Briefly described|p14|||Age of metamorphism discussed.||||||
14547|Olia Gneiss|33468|6|Mentioned|p214|||Metamorphic equiv.||||||
14547|Olia Gneiss|33478|5|Briefly described|p451|||||||||
14547|Olia Gneiss|34537|6|Mentioned|p43|||||||||
14547|Olia Gneiss|35102|6|Mentioned|p1|||||||||
14547|Olia Gneiss|35308|5|Briefly described|p451|||||||||
14547|Olia Gneiss|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
14547|Olia Gneiss|36887|5|Briefly described|p208|||||||||
14547|Olia Gneiss|40740|6|Mentioned|p1|||||||||
14547|Olia Gneiss|41723|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
14547|Olia Gneiss|42504|6|Mentioned|p67|||||||||
14547|Olia Gneiss|42794|6|Mentioned|p3|||||||||
14547|Olia Gneiss|42844|6|Mentioned|p469|||||||||
14547|Olia Gneiss|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|Gneiss, granite, schist.  Geological province: Musgrave Block.||||||07-NOV-08
14547|Olia Gneiss|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, granulite. Geological Province: Musgrave Block.||||||07-NOV-08
14547|Olia Gneiss|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14547|Olia Gneiss|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
14547|Olia Gneiss|43697|6|Mentioned|p27|||||||||
14547|Olia Gneiss|44109|5|Briefly described|p164, p157|Mesoproterozoic|Mesoproterozoic|Age: <1600Ma. See also p165 Fig. 163C and p166 Fig. 164.||||||
14547|Olia Gneiss|44139|5|Briefly described|p283, 285 Fig. 3-69, p286|||Wells et al. (1970). Of Wingelina Complex. Fine- to medium-grained banded quartzofeldspathic gneiss, and intrusions of porphyritic granite; all at amphibolite facies. Occurs in northern Wingelina Complex below Woodroffe Thrust. Unconformably overlain by Dean Quartzite.|| ||||06-MAR-18
14547|Olia Gneiss|44493|4|Described|p.7, map||Precambrian|BLOOD RANGE sheet (G53-3).||||||21-NOV-06
14547|Olia Gneiss|44494|14|Not recorded|map legend||Precambrian|Undifferentiated.||||||
14547|Olia Gneiss|44495|4|Described|p.4,5, map||Precambrian|AYERS ROCK sheet (G52-8). See p.7,9, for details.||||||21-NOV-06
14547|Olia Gneiss|44496|5|Briefly described|map legend||Precambrian|Gneiss with schist, porphyroblastic schist, amphibolite, migmatite and granite.||||||10-JUL-13
14547|Olia Gneiss|45041|5|Briefly described|p14|||Precamb. Refers Forman (1966)||||||
14547|Olia Gneiss|45085|6|Mentioned|p14|||Age of metamorphism.||||||
14547|Olia Gneiss|45170|6|Mentioned|p5|||||||||
14547|Olia Gneiss|48864|2|Defined|p.17,18||Neoproterozoic|Tb.1. On many pages. p.16,22,28,29,33,39,41,42,44,52,Pl.9,11-13, (G52-3,7,8).late U.Prot.||||||
14547|Olia Gneiss|48963|6|Mentioned|p3|||||||||
14547|Olia Gneiss|49833|6|Mentioned|p8|||||||||
14547|Olia Gneiss|50607|5|Briefly described|p1.1, 2.2|||Geological Province: Musgrave Block. Of the Kulgera Supersuite.||||||
14547|Olia Gneiss|60662|5|Briefly described|Map legend|||Layered to massive amphibolite facies gneisses.||||||22-FEB-05
14547|Olia Gneiss|60683|5|Briefly described|p55 Appendix|||Originally of Forman (1966a, 1972).  Replaced by Umutju Granite Suite (Matapayika Granite), Pottoyu Granite Suite (Mulyatti Granite) and Mantarurr Granite Suite (Kulu, Foster Cliff and Wala Wuru Granites). Overlain by Bloods Range beds and Dean Quartzite.||||||
14547|Olia Gneiss|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: >1607Ma (metamorphic age). Amphibolite facies gneiss, minor pelitic schist.||||||07-NOV-08
14547|Olia Gneiss|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Gneiss, amphibolite-facies; minor pelitic schist. Age: >1607 Ma (metamorphic age).||||||07-NOV-08
14547|Olia Gneiss|61154|6|Mentioned|p4|||See also "Olia Gneiss".||||||
14547|Olia Gneiss|61306|6|Mentioned|p61|||Geological Province: Amadeus Basin.||||||
14547|Olia Gneiss|62609|5|Briefly described|Map Legend|Precambrian|Precambrian|Gneiss, granite, schist.||||||
14547|Olia Gneiss|62620|5|Briefly described|Map Legend|Precambrian|Precambrian|Gneiss, granite, schist.||||||
14547|Olia Gneiss|64745|5|Briefly described|p373 Fig. 3|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Mulga Park Domain, Musgrave Province. See Olia gneiss.||||||
14547|Olia Gneiss|65376|6|Mentioned|p9 Fig.1.2. |Paleoproterozoic|Paleoproterozoic|||||||
14547|Olia Gneiss|67536|6|Mentioned|Map Legend|||Musgrave Block. Informally subdivided into three parts.|||||Altered, sheared, demagnetised gneiss adjacent to major shear zones, weakly magnetic; layered gneiss, moderately to strongly magnetic; massive or poorly-banded gneiss, moderately magnetic.|
14547|Olia Gneiss|68100|5|Briefly described|p6 |||Of Major and Conor (1993). Mulga Park Domain. Not correlated with Birksgate Complex. Ages of granitic protoliths up to 1591 Ma.|||||Orthogneiss, paragneiss, gneisses, often with granitic protoliths.|19-JAN-17
14547|Olia Gneiss|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Gneiss.|
14547|Olia Gneiss|69926|6|Mentioned|p156|||Forman (1972). Eastern Musgrave Block.|||||Amphibolite facies rocks.|
14547|Olia Gneiss|70083|6|Mentioned|p206|||The name used for the Musgravian Gneiss in the Mulga Park Subdomain, Eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Birksgate Complex in the Fregon Subdomain.||||||
14547|Olia Gneiss|71210|6|Mentioned|p3, p7|||||||||
14547|Olia Gneiss|71211|6|Mentioned|p228|Mesoproterozoic|Mesoproterozoic|Metamorphosed at 1220-1150 Ma during the Musgravian Orogeny.|1600-1540 Ma||||Felsic gneiss with interlayered and subordinate mafic units and rare metapelite.|
14550|Oliver Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p229|Pliocene|Miocene|In figure, Fm = Formation. Includes Oliver Sand Member. Geological Province: Bonaparte Basin. Composed of firm to moderately hard calcarenites with abundant skeletal material.||||||01-MAR-10
14550|Oliver Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Neogene|Browse Basin.||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13353|6|Mentioned|p401 Fig.2.|Neogene|Neogene|||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Neogene|Unit of Woodbine Group. Overlies Cartier Formation and underlies Barracouta Formation.||86||||28-OCT-14
14550|Oliver Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Miocene|Of the Woodbine Group.||||||01-MAR-10
14550|Oliver Formation|23377|4|Described|p212 Fig.5; p218|Quaternary|Miocene|In the Vulcan Sub-basin. Unconformable base.||||||21-NOV-06
14550|Oliver Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
14550|Oliver Formation|24218|5|Briefly described|p847|Early Miocene|Early Miocene|Geological Province: Bonaparte Basin.||||||
14550|Oliver Formation|42053|5|Briefly described|Fig.2 P29|||See also Fig.2||||||01-MAR-10
14550|Oliver Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
14550|Oliver Formation|60634|6|Mentioned|p1168 Fig.3. |Miocene|Miocene|||Unit in Woodbine Group.||Overlies Prion Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|61548|6|Mentioned|p480 Fig.3|Miocene|Miocene|Northern Bonaparte Basin.||||||
14550|Oliver Formation|61550|6|Mentioned|p495 Fig.2. |||||Unit in Woodbine Group.||Is overlain by Barracouta Formation.||
14550|Oliver Formation|62837|5|Briefly described|Stratigraphic columns|Late Miocene|Oligocene|Contains the Oliver Sand Member. Age: ~25-~7.0Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
14550|Oliver Formation|63358|5|Briefly described|p4 Fig. 1.3|Miocene|Miocene|||||||01-MAR-10
14550|Oliver Formation|64695|5|Briefly described|p260-262  |Miocene|Miocene|Northern Bonaparte Basin.|||Includes Oliver Sandstone Member.|Unconformably overlies Prion and Hibernia Formations. Is overlain by Barracouta Formation.||
14550|Oliver Formation|64697|5|Briefly described|p84 Fig.2 |Miocene|Miocene|||||||
14550|Oliver Formation|65680|6|Mentioned|p709 Fig.2.|Messinian|Aquitanian|Host to an interpreted dish-shaped, multiringed impact structure, about 2.5 km diameter, formed by collision of a meteorite or small asteroid with unconsolidated, water-saturated shallow-marine shelf carbonate, in mid- to late-Serravallian.|||Includes Oliver Sandstone Member.|Overlies Cartier Formation. Is unconformably overlain by Barracouta Formation.||
14550|Oliver Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1, p421, p423|Miocene|Oligocene|Unit in Woodbine Group. Underlies Barracouta Formation (WA), overlies the Prion Formation unconformably. In the Mount Ashmore Dome. Mainly limestone and dolomite.||||||
14550|Oliver Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4, p184 Fig.9|Miocene|Miocene|In Fig. 9, the base of Pliocene is indicated by the Top Oliver Formation.||||||
14550|Oliver Formation|69297|6|Mentioned|p305|Messinian|Chattian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Woodbine Group||Overlies the Cartier Formation. Overlain by the Barracouta Shoal Formation.||
14550|Oliver Formation|69452|5|Briefly described|p36:15, 22|Neogene|Neogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
14550|Oliver Formation|69673|6|Mentioned|p174|||||||||
14550|Oliver Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Miocene|Oligocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2, p2. Reservoir. Sealed by intraformational carbonates or the overlying Barracouta Shoal Formation.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
14550|Oliver Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Miocene|Oligocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
14551|Oliver Twist Granodiorite|42382|4|Described|p41|||Related to Oliver Formation??||||||
14551|Oliver Twist Granodiorite|42742|5|Briefly described|map legend|Archean||||||||07-NOV-08
14551|Oliver Twist Granodiorite|43074|5|Briefly described|p19,p30.|||||||||
14551|Oliver Twist Granodiorite|50075|5|Briefly described|p18|Archean|Archean|Geological Province: Yilgarn Craton.||||||23-DEC-09
14551|Oliver Twist Granodiorite|50076|5|Briefly described|Map|Archean|Archean|Biotite-hornblende granodiorite.  Geological Province: Yilgarn Craton.||||||07-NOV-08
14551|Oliver Twist Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggot]   Biotite granodiorite; locally monzogranitic.||||||
14551|Oliver Twist Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite granodiorite, local monzogranite; domal within D2 antiform; sheared contacts with greenstones.|06-AUG-15
14551|Oliver Twist Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite granodiorite, local monzogranite; domal within D2 antiform; sheared contacts with greenstones.|
14551|Oliver Twist Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granodiorite|
14551|Oliver Twist 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.|2817-2600 Ma (inferred)||||Biotite granodiorite, local monzogranite; metamorphosed|
14563|Olympic Formation|14019|6|Mentioned|p19|||Geological Province: Amadeus Basin.  Correlated with Fargoo Tillite (Grey and Corkeran, 1998).||||||
14563|Olympic Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Cryogenian|||||||
14563|Olympic Formation|22560|6|Mentioned|p2|||||||||
14563|Olympic Formation|22561|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22566|4|Described|p81|Neoproterozoic|Neoproterozoic|Stratigraphic relations described from a number of localities - p81.  Type section mentioned, thickness and distribution discused - p81.||||||
14563|Olympic Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
14563|Olympic Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22648|4|Described|p 127 - 132|Neoproterozoic|Neoproterozoic|||||||13-NOV-06
14563|Olympic Formation|22649|4|Described|p 143|Neoproterozoic|Neoproterozoic|At the type section for the Gaylad Sandstone the Olympic Formation is 36 meters thick,  the Olympic Formation is overlain by Gaylad Sandstone and underlain by the Loves Creek Member of the Bitter Springs Formation.||||||21-NOV-06
14563|Olympic Formation|22651|6|Mentioned|Fig 11 btw p182-183|Proterozoic|Proterozoic|||||||
14563|Olympic Formation|22762|5|Briefly described|p374|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22804|5|Briefly described|p440|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|23250|5|Briefly described|p1124  Fig.2||Cryogenian|Correlate of Whyalla Sandstone and Wilmington Formation equivalent and Elatina Formation, Yaltipena Formation and Trezona Formation (Umberatana Group). Geological province: Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|23287|6|Mentioned|Fig.4|||Age: Upper Cryogenian. In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|23314|5|Briefly described|333 Fig.4|Neoproterozoic III||Geological province: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Cryogenian|||||||
14563|Olympic Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
14563|Olympic Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. See also p215 Fig. 11.||||||
14563|Olympic Formation|24442|6|Mentioned|p38|||Geological Province: Centralian Superbasin.||||||
14563|Olympic Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
14563|Olympic Formation|35863|6|Mentioned|Table 1|||||||||
14563|Olympic Formation|36898|6|Mentioned|p181, p195 Fig. 4, p198|||Red, silty, dolomitic. Geological province: eastern Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|37462|4|Described|Table 4.IX|||||||||
14563|Olympic Formation|37928|3|Fully described|p517|||||||||
14563|Olympic Formation|37929|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|38157|6|Mentioned|Table VI|||||||||
14563|Olympic Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|38945|6|Mentioned|p130|||Includes diamictites. Geological Province: Amadeus Basin (NT).||||||16-NOV-06
14563|Olympic Formation|39565|6|Mentioned|p32|||||||||
14563|Olympic Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
14563|Olympic Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite, overlain by green shale with scattered boulders. Geological Province: Amadeus Basin.||||||14-FEB-06
14563|Olympic Formation|40740|4|Described|p12|||||||||
14563|Olympic Formation|40810|6|Mentioned|p3|||||||||
14563|Olympic Formation|40852|6|Mentioned|p24 Fig. 3.2, p29|Adelaidean|Adelaidean|Geological province: Amadeus Basin.  Correlation with Wilpena Group in the Adelaide Geosyncline is suggested (Preiss et al 1978).||||||16-NOV-06
14563|Olympic Formation|40906|6|Mentioned|Fig.9|||||||||
14563|Olympic Formation|41005|6|Mentioned|p419 Fig.2|||Age: Marinoan. Geological Province: Amadeus Basin in NT.||||||16-NOV-06
14563|Olympic Formation|41039|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|41190|6|Mentioned|Fig.4|||||||||
14563|Olympic Formation|41270|6|Mentioned|Table 1|||||||||
14563|Olympic Formation|41405|5|Briefly described|p205|||Capped by laminated pink dolomite identical to that of Nuccaleena Fm. Incl: upper lenticular boulder tillite, gritty pebbly dolomite; lower red siltstone with interbedded lenses of dark limestone and gritty to pebbly limestone. Geol. prov: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|41429|5|Briefly described|p246|||Thin laminated pink to buff dolomite capping Marinoan tillites.  Geological province: Amadeus Basin.  Equivalent to Nuccaleena Formation.||||||16-NOV-06
14563|Olympic Formation|41618|6|Mentioned|Fig.2|||Glacigenic unit. geological province: Amadeus Basin.||||||22-NOV-06
14563|Olympic Formation|41717|6|Mentioned|Fig.2|||||||||
14563|Olympic Formation|41801|6|Mentioned|Fig.4|||||||||
14563|Olympic Formation|41852|6|Mentioned|p210|||||||||
14563|Olympic Formation|42059|6|Mentioned|Fig.2 P131|||||||||
14563|Olympic Formation|42082|6|Mentioned|Fig.3 P323|||||||||
14563|Olympic Formation|42504|5|Briefly described|p72|||||||||
14563|Olympic Formation|42643|6|Mentioned|p21|||In the Amadeus Basin.||||||21-NOV-06
14563|Olympic Formation|42845|6|Mentioned|Fig.3 P498|||||||||
14563|Olympic Formation|42886|5|Briefly described|Fig.2 P219|||see also Fig.1 p218.||||||21-NOV-06
14563|Olympic Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Diamictite, sandstone, shale, limestone.  Geological province: Amadeus Basin.||||||23-JAN-08
14563|Olympic Formation|43105|5|Briefly described|Fig.3,p8|||||||||
14563|Olympic Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
14563|Olympic Formation|43595|5|Briefly described|p548, p549 Fig5-33|Adelaidean|Adelaidean|Age: 660-680 Ma. Geological province: Amadeus Basin.||||||16-NOV-06
14563|Olympic Formation|43756|6|Mentioned|p542|||||||||
14563|Olympic Formation|44111|6|Mentioned|p.58 Fig. 2|||in Amadeus Basin, presented as "Olympic" only in Fig. 2.||||||
14563|Olympic Formation|46865|6|Mentioned|p43|||Upgraded p51.||||||21-NOV-06
14563|Olympic Formation|46903|6|Mentioned|p54|||||||||
14563|Olympic Formation|49796|4|Described|p1 & Sections|||||||||
14563|Olympic Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite overlain by green shale.||||||
14563|Olympic Formation|60682|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||03-MAY-05
14563|Olympic Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
14563|Olympic Formation|61732|3|Fully described|p4 Fig. 3, p91-92.|Cryogenian|Cryogenian|Glacigenic rocks orginally defined as Olympic Member (Pertatataka Fm), but now upgraded to formation status. Unconformably on Aralka Fm. Max. thickness: 300m. Geol.Prov: Amadeus Basin. See also p5 Tb. 1, p31, p87.||||||07-FEB-11
14563|Olympic Formation|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Amadeus Basin. The base of the cap carbonate at the top of this unit corresponds with the Ediacaran GSSP.||||Intertongues with Gaylad Sandstone.||
14563|Olympic Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
14563|Olympic Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Amadeus Basin.||||||
14563|Olympic Formation|62903|5|Briefly described|p729, p730|||Amadeus Basin. Very thin stratigraphic thickness of Aralka Formation preserved in Wallara-1 (~27m) may be a lacuna unconformity between the Aralka and Olympic Formations. Presented as Olympic in figure.||||overlies hiatus overlying Aralka Formation, abrupt contact in drillcore; interpreted as Marinoan (Yerelina Subgroup) equivalent (Walter et al. 2000).|glacial|
14563|Olympic Formation|62984|5|Briefly described|p13|Cryogenian|Cryogenian|Geological Province: Amadeus Basin. Representative of the Marinoan glacial episode.||||||23-JAN-07
14563|Olympic Formation|63458|6|Mentioned|p873, p897 Fig.19, p900. |Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Aralka Formation. Correlated with Fargoo Tillite.||
14563|Olympic Formation|63562|5|Briefly described|p338 fig 3, p343-344, p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin.|||||Includes (Marinoan) diamictites.|
14563|Olympic Formation|64068|6|Mentioned|p46|||Amadeus Basin.  Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
14563|Olympic Formation|64103|6|Mentioned|p404|||Geological Province: Amadeus Basin.||||||07-FEB-11
14563|Olympic Formation|64625|5|Briefly described|p243, p245, p247, p252, p256-257|||Amadeus Basin. Correlated with Marinoan glacial event. Lithology, C and O isotopes detailed.||||Overlies Bitter Springs Formation, and Aralka Formation unconformably. Unconformably overlain by Gaylad Sandstone.|Green mudstone, pebbly sandstone and conglomerate, breccia, dolomite beds and diamictite; thin-bedded sandstone and dolomite, massive chert-bearing dolomite.|
14563|Olympic Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|64797|6|Mentioned|p153 Fig.2, p164 Fig.11|Ediacaran|Ediacaran|Amadeus Basin. Rank not shown in diagram; shown as Olympic Boord.||||||
14563|Olympic Formation|64809|5|Briefly described|p3 Fig.2, p15 Fig.15 |Proterozoic|Proterozoic||||||Dolostone, conglomerate, sandstone.|
14563|Olympic Formation|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Tog. with Pioneer Sst. disconformably overlies Aralka Fm.Max. thickness: 190m. Geol.prov: Amadeus Basin. Lenticular units of sst., siltst., conglom/diamictite, shale+dolostone in NE of basin. Lateral equiv. is Pioneer Sandstone.||||||07-FEB-11
14563|Olympic Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
14563|Olympic Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Amadeus Basin||||||
14563|Olympic Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Amadeus Basin||||||
14563|Olympic Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3.||||||
14563|Olympic Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. 190m thick. The diamictite is associated with the Marinoan glaciation.||||Disconformably overlies Aralka Formation. Is overlain unconformably by Gaylad Sandstone.|Red and green siltstone and sandstone, pebbly arkose and conglomerate, and dark red-brown diamictite.|
14563|Olympic Formation|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Pioneer Sandstone.||
14563|Olympic Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Amadeus Basin.||||Overlain by the Pertatataka Formation. Underlain by the Aralka Formation.||
14563|Olympic Formation|67565|6|Mentioned|p5 Fig.3.|||Amadeus Basin.||||||
14563|Olympic Formation|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Pertatataka Formation.||
14563|Olympic Formation|67856|5|Briefly described|p338 fig 4-30, p345|Neoproterozoic|Neoproterozoic|Shown as equivalent to Pioneer Sandstone.||||Underlies Pertatataka Formation.||
14563|Olympic Formation|68244|6|Mentioned|p671|||Amadeus Basin.||||||
14563|Olympic Formation|68270|4|Described|p679,682-683,685-688|Cryogenian|Cryogenian|Amadeus Basin. Type section occurs 8 km SE of Ringwood Homestead; lat. 23'54"S, long.,134'59"E. Restricted to the NE Amadeus Basin. Less than 200m thick. Periglacial: fluvial to marginal marine deposit. Clasts are mainly fine-coarse pebbles, range up to boulder size in the upper parts of the formation. Clasts are mostly rounded and consist of quartzite, granite, gneiss, carbonate and basalt; some are faceted. Includes a paraconformable, up to 30m thick (4m in type section) "upper marker cap dolomite" intersected in type area, and is related to Elatina glaciation. Correlable to Elatina Formation, Nuccaleena Formation.||||Overlain by Pertatataka Formation, Underlain disconformably by Aralka Formation.|Red and green mudstone and siltstone with intercalated sandstone, diamictite, siltstone, conglomerate and dolomite (which generally overlie conglomerate).|03-JUL-19
14563|Olympic Formation|68276|5|Briefly described|p68, 73|Neoproterozoic|Neoproterozoic|Amadeus Basin. The ""Formation"" is omitted.",,||||Is overlain conformably by Pertatataka Formation.|Glaciogenic deposits, overlain by seafloor barite associated with ferruginous domal stromatolites.|
14563|Olympic Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
14563|Olympic Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
14563|Olympic Formation|68733|5|Briefly described|p188, p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.|||||Diamictites.|05-DEC-17
14563|Olympic Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
14563|Olympic Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Aralka Formation. Is overlain by Gaylad Sandstone. Is equivalent to Pioneer Sandstone.|Diamictite, siliciclastic rocks and dolostone.|12-JUL-16
14563|Olympic Formation|69438|4|Described|p23:2-5, 16-19, 43|Ediacaran|Cryogenian|Priess et al. (1978); previously the Olympic Member of the Pertatataka Formation (Wells et al., 1967). Amadeus Basin. Up to 190m thick. Has been correlated with the diamictite member of the Mount Doreen Formation (Ngalia Basin); Oorabra Arkose, Boko Formation, Black Stump Arkose (Georgina Basin); Chambers Bluff Tillite (Officer Basin). The "cap dolostone" has been correlated with the Nuccaleena Dolostone (Adelaide Fold Belt).||||Disconformably overlies Aralka Formation. Lateral equivalent of Pioneer Sandstone. Is overlain disconformably by Pertatataka Formation.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone. Near the top is a pale brown and pink gritty dolostone ("upper marker cap dolomite") which is a laminated, thinly bedded interval up to 30m thick.|12-JUL-16
14563|Olympic Formation|69439|6|Mentioned|p24:8|||Amadeus Basin.||||Correlated with Mount Davenport Diamictite Member.||12-JUL-16
14563|Olympic Formation|69441|6|Mentioned|p26:1|||Amadeus Basin.||||Correlated with Moonlight Valley Tillite (Wolfe Basin).||12-JUL-16
14563|Olympic Formation|69442|6|Mentioned|p27:4|||Amadeus Basin.||||Correlated with Fargoo Tillite (Wolfe Basin).||12-JUL-16
14563|Olympic Formation|69443|5|Briefly described|p28:8|||Adelaide Fold Belt. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation.||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
14563|Olympic Formation|69606|5|Briefly described|p1, p4 fig 2, p5, p6 fig 3, p7 fig 4|Cryogenian|Cryogenian|Supersequence 3. <100m thick. Potential reservoir and seal rock. Amadeus Basin. Poorly exposed. Glacigene origin, inferred to have been deposited during the Elatina glaciation. Previously the Olympic Member of Wells et al, 1967.  See also p12, p13 fig 7, p14, p19.||||Overlies the Aralka Formation, overlain by the Pertatataka Formation. Inferred to be equivalent to the Pioneer Sandstone.|The dominant lithology is siltstone with interbedded sandstone, while conglomerate, lesser dolostone and reddish glacial diamictite with striated and faceted clasts as smaller components.|
14563|Olympic Formation|69673|5|Briefly described|p63, p64 fig 53, p88, p91|||Potential reservoir rock.||||Overlain by Pioneer Sandstone, disconformably overlies Aralka Formation|Diamictite, siliciclastic rocks and dolostone.|
14563|Olympic Formation|69937|4|Described|v Fig.1, vi, p3 Tb.1, p17-19, p22, p26|Neoproterozoic|Neoproterozoic|See also p45-46. NE Amadeus Basin. Formerly the Olympic Member of Pertatataka Formation (Wells et al., 1967). A potential equivalent to the Pioneer Sandstone. Correlated with the ~640 Ma to ~580 Ma Elatina glacial succession. Likely zircon provenance discussed.|690 +/- 14 Ma (maximum depositional age).|||Disconformably overlies Areyonga and Aralka Formations. Is overlain unconformably by Waldo Pedlar Member (Pertatataka Formation). Lateral equivalent of Pioneer Sandstone.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone.|
14563|Olympic Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Equivalent to Pioneer Sandstone. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation.||
14563|Olympic Formation|70416|5|Briefly described|p63, p65, p68, p72, p74, p80|Cryogenian|Cryogenian|Deposited during the Elatina Glaciation. Contains reworked stromatolite Tungussia inna from the underlying Aralka Formation.||||Unconformably overlies Aralka Formation. Is overlain by Pertatataka Formation. Laterally equivalent to Pioneer Sandstone.||
14563|Olympic Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation. Equivalent to Pioneer Sandstone.||
14563|Olympic Formation|71001|5|Briefly described|p18 Fig.2, p19-21, 23, 27-28|Cryogenian|Cryogenian|Amadeus Basin. Glacial deposits. Cap carbonate is dominated by manganiferous dolomite. Carbon isotope correlation graph.||||Overlies Aralka Formation. Is overlain by Gaylad Sandstone.|Glacial sandstone; cap carbonate.|
14563|Olympic Formation|71080|5|Briefly described|p27, p29 fig 20, p30|Cryogenian|Cryogenian|Amadeus Basin. Supersequence 3. Includes glacial diamictites?|||||Diamictite, sandstone and lesser conglomerate.|
14563|Olympic Formation|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
14563|Olympic Formation|71279|5|Briefly described|p355 Fig.2, p382 Tb.1|Ediacaran|Cryogenian|Amadeus Basin. Modelled magnetic properties.||||||
14563|Olympic Formation|71344|5|Briefly described|p1094, 1096-1100, 1102-3|||Amadeus Basin.  Glaciogenic succession. Top commonly marked by a pink cap carbonate that in some places contains small columnar stromatolites.||Of Inindia Package.||Unconformably overlies the Aralka Formation. Equivalent to Pioneer Sandstone. Is overlain conformably by Pertatataka Formation.|Conglomerates, diamictites, sandstones, shales and carbonates.|10-NOV-17
14563|Olympic Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|690+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse-grained feldspathic sandstone.|
14563|Olympic Formation|71801|6|Mentioned|p230-p231, p237|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Aralka Formation.||
14563|Olympic Formation|71810|5|Briefly described|Map legend.|Ediacaran|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Diamictite, sandstone, conglomerate, and siltstone; large erratics; common glacially faceted and striated clasts.|
14563|Olympic Formation|71841|5|Briefly described|p1|Ediacaran|Cryogenian|Of Amadeus Basin.||||Equivalent to Pioneer Sandstone. Grades into Inindia beds.||
14563|Olympic Formation|71842|5|Briefly described|p1-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Generally confined to the NE Amadeus Basin, and disappears from outcrop westward from central northern margin.||||Equivalent with Pioneer Formation. Overlain by Pertatataka Formation. Underlain by Aralka Formation. Correlable with Winnall beds.||
14563|Olympic Formation|72369|5|Briefly described|p7,9-10|||Of Amadeus Basin.||||Underlain disconformably by Aralka Formation.||
14563|Olympic Formation|72375|4|Described|p1-2,19-23,25|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Formerly known as Olympic Member of the Pertatataka Formation (Wells et al., 1967). Redefined (Priess et al 1978). Restricted to the NE Amadeus Basin, and can be correlated with Elatina glacial successions of the Adelaide Rift Complex and the Georgina, Ngalia and Officer basins (Lindsay 1993, Walter et al 1995). SHRIMP U-Pb zircon analyses by Kositcin et al., 2015 yielded an interpreted maximum depositional age (pooled 238U/206Pb) of 690+\-14 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations from NTGS RD13CJE001 (feldpsathic quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p21-22 for Hf isotopic results and interpretations). Sample location and description is provided.||||Overlain unconformably by Gaylad Sandstone or Pertatataka Formation. Underlain disconformably by Aralka Formation. Laterally correlable (interfingers with) to Pioneer Sandstone.|Lenticular units of sandstone, siltstone, conglomerate, diamictite, shale and dolostone.|04-DEC-19
14563|Olympic Formation|72489|5|Briefly described|p3, p4 Fig.3|Cryogenian|Cryogenian|Amadeus Basin.||||Unconformably overlying Aralka Formation.|Includes glacial deposits and also stromatolitic bioherms, oolitic grainstone, intraclast breccia, and packstone.|
14563|Olympic Formation|72601|5|Briefly described|p: 1, 3-5, 7-8, 11-12, 14, 16, 19, 24-25|Cryogenian|Cryogenian|Amadeus Basin. Deposition was coeval with the Elatina glaciation. Renamed from the Olympic Member. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Unconformably underlain by Aralka Formation. Overlain by Pertatataka Formation. Equivalent to Pioneer Sandstone. Correlates to Cottons Breccia.||
14563|Olympic Formation|73085|6|Mentioned|p1, p27|Ediacaran|Ediacaran|Previously thought to occur in drillhole BR05DD01 as what is now considered Areyonga Formation. [Unclear relationship with Pioneer Sandstone].||||Underlain by Aralka Formation. Partly overlain by[?] Pertatataka Formation unconformably. Partly overlain by[?] and equivalent to[?] Gaylad Sandstone. Equivalent to Inindia beds.||
14563|Olympic Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Added type area. Glaciogenic. Amadeus Basin. Part of Supersequence III. Diamictite includes intrabasinal clasts (i.e., Heavitree Formation, Bitter Springs Group, Aralka Formation, Areyonga Formation and less basement rock clasts than seen in Areyonga Formation diamictite). Can be difficult to distinguish from the Areyonga Formation based on lithology alone. When the diamictite is absent, it is difficult to differentiate from the Waldo Pedlar Member of the Pertatataka Formation. Cap carbonate is not ubiquitous. Lateral equivalent of the Pioneer Sandstone; less widely recognised in the subsuface than Pioneer Sandstone. Previously a member of the Pertatataka Formation. Age constrained by correlation with Chambers Bluff Tillite (Rb-Sr age of 651 +/- 87 Ma) and the ca 660-635 Ma Marinoan glaciation, supported by a 690 +/- 14 Ma detrital zircon maximum depositional age. No known fossils other than poorly preserved stromatolites. May preserve the Cryogenian-Ediacaran boundary. Partly overlain by [and equivalent to?] Gaylad Sandstone. Correlates with Mount Doreen Formation, Elatina Formation, Nuccaleena Formation, Oorabra Arkose, Black Stump Arkose, Boko Formation, Chambers Bluff Tillite, Pioneer Sandstone. p: 3, 5-6, 27-28, 53-54, 63, 67, 71-72, 79, 91, ~99-114, 118-123, 143, 160, 167-169, App 2.|ca. 650 Ma|||Unconformably underlain by Gillen and Johnnys Creek formations (Bitter Springs Group) and Aralka Formation. Unconformably overlain by Pertatataka Formation. [See comments for more].|Glacial deposits including lenticular diamictite, sandstone, siltstone, conglomerate, boulder clay, and dolostone in varying proportions with rapid lateral variation in thickness and lithology.|
14563|Olympic Formation|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Unconformably underlain by Aralka Formation. Overlain by Gaylad Sandstone. Equivalent to Pioneer Sandstone.||
14563|Olympic Formation|73180|4|Described|p47-48 p52-54|Neoproterozoic|Neoproterozoic|Amadeus Basin. Defined by Preiss et al (1978). Elatina glacial/post-glacial sequences. Outcrop limited to the northeast of the basin and the Boord Ridges. Disconformable contact with Bitter Springs Group in the north and northeast of the basin from erosion by a grounded ice sheet, deposition of thin sandstones and conglomerates from localised high-energy deposition, likely glacial outwash.||||Equivalent to the Pioneer Sandstone, disconformably overlies the Aralka Formation, conformably underlies the Pertatataka Formation.|Glaciogenic suite of lenticular diamictites, polymict conglomerates, pebbly arkosic sandstones, siltstones and mudstones with interbedded and overlying pink, commonly stromatolitic dolostones. Includes reworked carbonates.|
14567|Olympio Formation|505|6|Mentioned|p711|Archean|Archean|Halls Creek Province.||Of Halls Creek Group.|||Metasediments.|
14567|Olympio Formation|22496|3|Fully described|p8|Orosirian|Orosirian|Age of alkaline volcanic rocks (Maude Headley Member) 1857 +/- 3 Ma, and overlying Butchers Gully Member 1848+/-3 Ma. Halls Creek Group, Halls Creek Province, overlies Biscay Formation, overlain by Ruby Plains Group.||||||20-FEB-17
14567|Olympio Formation|22526|4|Described|P680, Fig3 P682||Orosirian|Age of unit is 1847+/-6 Ma.||||||21-NOV-06
14567|Olympio Formation|22547|6|Mentioned|p9||Orosirian|Of the Halls Creek Group.||||||14-NOV-06
14567|Olympio Formation|22716|6|Mentioned|p234|||||||||
14567|Olympio Formation|22754|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group. Age c. 1870-1840 Ma.||||||07-NOV-08
14567|Olympio Formation|22764|4|Described|Table1,p7|Paleoproterozoic|Archean|Also p 5. Halls Creek Group||||||01-FEB-10
14567|Olympio Formation|22777|5|Briefly described|Map|||||||||
14567|Olympio Formation|23314|5|Briefly described|p332, p333|Paleoproterozoic|Paleoproterozoic|Tightly folded unit. Overlain by Illjarra Sandstone and by Mount Kinahan Sandstone. Age: ca1850Ma.  In the Halls Creek Orogen.||||||07-NOV-08
14567|Olympio Formation|23323|6|Mentioned|p455|||||||||07-FEB-07
14567|Olympio Formation|23383|4|Described|p12, p5 Tb. 1|||Of Halls Creek Gp. Contains Maude Headley Mbr. Monotonous sequence of weakly metamoprhosed, thin- to medium-bedded mudstone, siltstone, and matrix-supported quartz wacke, greywacke and arkose. Age: <1847Ma. Max. thickness 4000 m. Geol.Prov: Hooper Orogen.||||||25-JAN-05
14567|Olympio Formation|23599|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group. Underlain by Biscay Formation. Geological Province: Lamboo Complex. Max. thickness: 4000 m.||||||07-NOV-08
14567|Olympio Formation|23601|5|Briefly described|Map legend|||Of Halls Creek Group.  very low to low grade, thin to medium bedded mudstone, siltstone, turbiditic quartz wacke, greywacke, and arkosic sandstone.  Age: c.1860Ma.||||||25-JAN-05
14567|Olympio Formation|23602|6|Mentioned|p17|||||||||
14567|Olympio Formation|23621|3|Fully described|p16|Orosirian|Orosirian|See also page 11 table 1. Of Halls Creek Group. Underlain by Biscay Formation. Halls Creek Orogen. Max. thickness: >2000 m.||||||21-NOV-06
14567|Olympio Formation|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group.||||||07-NOV-08
14567|Olympio Formation|23897|6|Mentioned|p394 Tb.7|||||||||
14567|Olympio Formation|24173|3|Fully described|p16, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Gp. Mainly turbiditic greywacke, siltstone and mudstone.  Incl: Maude Headley Mbr, Butchers Gully Mbr. Unconformable under Moola Bulla Fm; overlies Biscay Fm. Max Thickness: >1000m. Max. depositional age from detrital zircons in greywacke: 1873+/-5 Ma. AAge of volcanics in Maude Headley Fm: 1847 +/- 6Ma.||||||22-FEB-17
14567|Olympio Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group (Lamboo Complex).  Metamorphosed (low- to medium-grade) interbedded mudstone and siltstone, and turbiditic wacke, quartz wacke and arkosic sandstone.||||||07-NOV-08
14567|Olympio Formation|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group.  Metamorphosed sedimentary rocks.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
14567|Olympio Formation|29813|4|Described|Table 2|||||||||
14567|Olympio Formation|29818|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
14567|Olympio Formation|30097|6|Mentioned|Fig.54|||Also Tables 23,24,26||||||
14567|Olympio Formation|30533|6|Mentioned|p13|||Top unit in Halls Creek Group. Overlain by Whitewater Volcanics.||||||16-NOV-06
14567|Olympio Formation|30892|5|Briefly described|p94|||Archaean ?||||||
14567|Olympio Formation|30895|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean or Lower Proterozoic||||||07-NOV-08
14567|Olympio Formation|30896|6|Mentioned|p9|||Correlation||||||
14567|Olympio Formation|32660|5|Briefly described|Table 1|||||||||
14567|Olympio Formation|32728|5|Briefly described|Table 3|||||||||
14567|Olympio Formation|33443|6|Mentioned|p260|||||||||
14567|Olympio Formation|35120|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Proterozoic||||||07-NOV-08
14567|Olympio Formation|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14567|Olympio Formation|36551|6|Mentioned|p25|||||||||
14567|Olympio Formation|36885|4|Described|p166|||||||||
14567|Olympio Formation|36902|6|Mentioned|p11|||Unit of the Halls Creek Group.||||||16-NOV-06
14567|Olympio Formation|37462|4|Described|Table 4.I|||||||||
14567|Olympio Formation|38482|6|Mentioned|Table 1|||||||||
14567|Olympio Formation|40105|6|Mentioned|p311|||||||||
14567|Olympio Formation|41987|6|Mentioned|Fig.3, P73|||Originally entered as Olympic Formation. CEBMay95||||||
14567|Olympio Formation|41997|6|Mentioned|Fig.3 P73|||||||||
14567|Olympio Formation|42149|6|Mentioned|p703|||||||||
14567|Olympio Formation|42326|6|Mentioned|p9|||||||||
14567|Olympio Formation|42768|5|Briefly described|p6|||Of the Halls Creek Group.||||||21-NOV-06
14567|Olympio Formation|42811|6|Mentioned|p5|||Of the Halls Creek Group.||||||21-NOV-06
14567|Olympio Formation|42814|6|Mentioned|p5|||Of the Halls Creek Group.||||||21-NOV-06
14567|Olympio Formation|43299|5|Briefly described|Map Legend||Paleoproterozoic|Of the Halls Creek Group.||||||07-NOV-08
14567|Olympio Formation|43303|5|Briefly described|Map Legend||Paleoproterozoic|of Halls Creek Group. Age is about 1850 Ma.||||||07-NOV-08
14567|Olympio Formation|43632|6|Mentioned|p2|||||||||
14567|Olympio Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
14567|Olympio Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
14567|Olympio Formation|44155|4|Described|p234-238, p243 Tb.3-6|Paleoproterozoic|Paleoproterozoic|Turbidites: over 4km thick. Probably formed a single lithostratigraphic unit in Hooper and Lamboo Complexes; likely to be diachronous. Prominent pre-tectonic mafic sills and dykes.||Halls Creek Group||Gradationally overlies Biscay Formation. Is intruded by Woodward Dolerite. Is overlain unconformably by Whitewater Volcanics.|Subgreywacke, siltstone; minor dolomite, acid volcanics.|
14567|Olympio Formation|44231|5|Briefly described|Map Legend||Proterozoic|Of the Halls Creek Group. Metamorphosed, low to medium grade, thin to medium bedded phyllite, quartz-muscovite (-biotite-chlorite-andalusite-garnet) pelitic rocks and turbiditic quartz wacke, greywacke, and arkosic psammitic rocks.||||||19-MAY-05
14567|Olympio Formation|44317|4|Described|Table 1|||Archaean or Proterozoic.||||||
14567|Olympio Formation|44318|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
14567|Olympio Formation|44324|14|Not recorded|p.5|||Tb.1, (Archaean or Proterozoic). Of Halls Creek Group.||||||
14567|Olympio Formation|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
14567|Olympio Formation|44366|14|Not recorded|p.8, Table 1|||Archaean or Proterozoic. Part of the Halls Creek Group.||||||21-NOV-06
14567|Olympio Formation|44367|14|Not recorded|map legend|||(Reprinted 1971). Part of Halls Creek Group.||||||21-NOV-06
14567|Olympio Formation|44397|14|Not recorded|p.21, Table 1|||Of the Halls Creek Group. Archaean or Proterozoic.||||||21-NOV-06
14567|Olympio Formation|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
14567|Olympio Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
14567|Olympio Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
14567|Olympio Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
14567|Olympio Formation|45047|2|Defined|p65|Paleoproterozoic|Paleoproterozoic|See also pp13-16.||||||07-NOV-08
14567|Olympio Formation|45048|6|Mentioned|p10|||Of the Halls Creek Group. See also Fig.13.||||||21-NOV-06
14567|Olympio Formation|45140|2|Defined|p13, p17, p25, Appx.p12-13|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1969). Halls Creek Province. Named after Olympio Creek. Reference area is the middle reaches of Parton River, N of Saunders Creek area. Over 1000m thick: probably several thousand metres. Forms undulating to low hilly terrain. Most exposures are iron-stained. Described as "a monotonous turbidite sequence of great extent and uniformity".|>1961+/- 27Ma (metamorphism age).|Halls Creek Group.||Conformably overlies Biscay FZ. Is overlain unconformably by Mount Parker Sandstone. Correlated with Killi Killi Beds.|Interbedded schistose and phyllitic greywacke and siltstone, phyllite, minor quartzite, and local calcsilicate lenses. Some beds show graded bedding.|
14567|Olympio Formation|46797|6|Mentioned|p80|||Dates given||||||
14567|Olympio Formation|50437|6|Mentioned|p3.1, 5.3|||Interbedded with Butchers Gully Suite.||||||
14567|Olympio Formation|50542|6|Mentioned|p105|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen.||||||07-FEB-11
14567|Olympio Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Halls Creek Group. Includes: Maude Headley Member. Metamorphosed (low-medium grade) thin to very thickly bedded, fine to coarse grained, turbiditic lithic sandstone, greywacke, quartz wacke and arkose sandstone, siltstone and mudstone.||||||
14567|Olympio Formation|60724|4|Described|p4, p8|||Of Halls Creek Group. Contains the Butchers Gully Member. Monotonous succession of graded, fine to medium grained quartz wacke, greywacke, and arkosic sandstone. Overlies the Biscay Formation. Intruded by Woodward Dolerite. Within the Lamboo Complex.||||||
14567|Olympio Formation|61056|5|Briefly described|p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1857+/-2Ma.||||||07-NOV-08
14567|Olympio Formation|61861|5|Briefly described|p13, Fig.2.|||Eastern zone of the Halls Creek Orogen. The upper portion is similar to the Killi Killi Formation of Tanami Region.||Unit in Halls Creek Group?||Overlies Biscay Formation.||
14567|Olympio Formation|62377|5|Briefly described|p21|||In the Halls Creek region. Correlated with Killi Killi Formation.||||||
14567|Olympio Formation|63261|6|Mentioned|p23|||Upper section is a time-equivalent in the Halls Creek Orogen, of the Killi Killi Formation (Tanami region) and Lander Rock beds (Arunta region).||||||07-FEB-11
14567|Olympio Formation|63866|5|Briefly described|p130||||<1910 Ma|Halls Creek Group|Includes the Maude Headley Member and the Butchers Gully Member.||Low to medium grade turbiditic greywacke, quartz wacke, siltstone and arkosic sandstone.|
14567|Olympio Formation|64104|6|Mentioned|p63 Fig.1, p77 fig 11|Paleoproterozoic|Paleoproterozoic|||Halls Creek Group.||Is overlain unconformably by Duerdin Group.||
14567|Olympio Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Interbedded mudstone and siltstone, and feldspathic wacke, quartz wacke, and arkosic sandstone; turbiditic; metamorphosed at greenschist to amphibolite facies.||||||09-DEC-08
14567|Olympio Formation|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|Of Eastern Zone of Halls Creek Orogen. Age from Biscay Formation member (?).|1856 +/- 5 Ma (Page & Hancock 1988).||Includes Biscay Formation.|||12-APR-12
14567|Olympio Formation|65413|6|Mentioned|p105 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
14567|Olympio Formation|66846|5|Briefly described|p549 Fig.2|Orosirian|Orosirian|Overlying Butchers Gully member and Maude Headley Volcanic Member. In the Eastern Zone of the Lamboo Complex.|||Includes Butchers Gully Member and Maude Headley Volcanic Member|Overlying Butchers Gully member and Maude Headley Volcanic Member.|Turbidites and alkaline volcanics.|
14567|Olympio Formation|67127|5|Briefly described|p85-86||||||Includes the Butchers Gully Member.||Includes tuffaceous sandstone, pyritic mudstone, sandstone and greywacke.|
14567|Olympio Formation|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||1840-1860 Ma||Includes Butchers Gully Member, Maude Headley Volcanic Member|||
14567|Olympio Formation|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).||||||
14567|Olympio Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut. Lamboo Complex. Low gravity, non-magnetic to strong linear anomalies.|c.1845 Ma.|Halls Creek Group|Includes Butchers Gully Member.||Interbedded mudstone and siltstone, and feldspathic wacke, quartz wacke, and arkosic sandstone; turbiditic; volcanic rocks; metamorphosed at greenschist to amphibolite facies.|
14567|Olympio Formation|69003|5|Briefly described|p5, p19, p61|||E zone, Lamboo Province, Halls Creek Orogen. In the Cummins Range, it is intruded by a diatreme which forms part of a small alkaline/carbonatite complex hosting REE and minor U.|c.1860-c.1840 Ma.|Halls Creek Group.|Butchers Gully, Maude Headley Volcanic, Members.|||
14567|Olympio Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Dates range from 1910+/-30 Ma, 1861+/-5 Ma, 1847+/-6 Ma 'This (last) very immature detrital zircon suite in the gritstone contains mainly euhedral zircon. This maximum depositional age is based on 20 analyses'.|Max.deposit 1847+/-6 Ma U/Pb SHRIMP|Halls Creek Group|Includes Butchers Gully Member, Maude Headley Member and 3 unnamed members.||Turbiditic lithic and feldspathic metasandstone, interbedded metamudstone and metasiltstone; thin to very thick bedded; minor pebbly metasandstone; locally abundant magnetite; grey metadolostone, commonly jaspilitic.|03-AUG-15
14567|Olympio Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Neoarchean|See also 500k_geologyp08_lut.csv, GA_geochron.csv.|2188-2327 Ma|Halls Creek Group|||Turbiditic lithic and feldspathic metasandstone, interbedded metamudstone and metasiltstone, metadolostone (commonly jaspilitic). Thickly bedded turbiditic quartz metasandstone, minor pelite.|
14567|Olympio Formation|69585|5|Briefly described|p2, p4|Orosirian|Orosirian|Eastern Lamboo Province. Active margin submarine fan systems and alkaline volcanic rocks.||Halls Creek Group.||Overlies Biscay Formation.||
14567|Olympio Formation|69587|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 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1857-1808 Ma (isotopic; inferred)|Unit of Halls Creek Group.|Includes Butchers Gully Member.||Turbiditic lithic and feldspathic metasandstone, and interbedded metamudstone and metasiltstone; thin to very thick bedded; minor pebbly metasandstone|
14567|Olympio Formation|69597|6|Mentioned|p5 fig 2b|||||||||
14567|Olympio 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, 100k_interpgeol_lut.csv.|1857-1808 Ma (Isotopic)|Unit of Halls Creek Group.|Includes Butchers Gully Member, Maude Headley Member.||Turbiditic lithic and feldspathic metasandstone, and interbedded metamudstone and metasiltstone; thin to very thick bedded, locally abundant magnetite; minor pebbly metasandstone, grey metadolostone, commonly jaspilitic; minor pelite|
14567|Olympio Formation|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv.|1808-1857 Ma|Halls Creek Group|Includes Butchers Gully Member, Maude Headley Member||Metadolostone, commonly jaspilitic. Turbiditic lithic and feldspathic metasandstone, interbedded metamudstone and metasiltstone, metadolostone and quartz metasandstone.|
14567|Olympio Formation|70731|5|Briefly described|p268,272-273|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Median density: 2430 kg/m3.||Unit of Halls Creek Group.||||
14567|Olympio Formation|70812|4|Described|p5-p6, p13, p19, p27, p29-p31, p38|Orosirian|Orosirian|Eastern Zone of the Halls Creek Orogen, Lamboo Province. Mineralisation is described. Potentially formed in a foreland basin setting.|c. 1850 Ma|Halls Creek Group|Includes the Butchers Gully Member.|Overlies the Biscay Formation.||
14567|Olympio Formation|70851|4|Described|p3-p4, p11-p12, p35-p36|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province. Rock properties are provided.|c. 1850 Ma|Halls Creek Group||Overlies the Biscay Formation.|Turbiditic sedimentary rocks.|
14567|Olympio Formation|71113|5|Briefly described|p96-98|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Represents a transition from passive to active margin by c. 1850 Ma.|1870-1840 Ma|Unit of Halls Creek Group.|Includes Butchers Gully and Maude Headley members.|Uppermost unit of Halls Creek Group. Underlain disconformably by Biscay Formation.|Turbiditic metasedimentary rocks.|
14567|Olympio Formation|71140|5|Briefly described|p96-97|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|1870-1840 Ma.|Halls Creek Group.|Butchers Gully, Maude Headley Members.|Disconformably overlies Biscay Formation.|Turbiditic rocks with trachyandesitic and trachytic rocks.|
14567|Olympio 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, 100k_interpgeol_lut.csv and geochron files.|1856+\-6 to 1808 Ma (isotopic, inferred)|Unit of Halls Creek Group.|Includes Butchers Gully Member, Maude Headley Member.|Underlain disconformably(?) by Biscay Formation.|Turbiditic lithic and feldspathic metasandstone, interbedded metamudstone and metasiltstone; minor pebbly metasandstone, grey metadolostone (jaspilitic), quartz metasandstone|
14567|Olympio Formation|71281|5|Briefly described|p422|||Eastern Zone, Lamboo Province.||Halls Creek Group.|||Metaturbidites intercalated with c.1856 Ma and c.1846 Ma active-margin alkaline volcanic rocks.|
14567|Olympio Formation|71397|3|Fully described|p1,3-5,7-8,16,22,25,32,38-42,44-48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Deposted in a deep marine environment. Greenschist facies turbiditic metasedimentary rocks interlayered with subaqueous to emergent volcanic and volcaniclastic rocks. Detrital zircons from the top of the exposed Olympio Formation indicate a maximum depositional age of 1834+\-8 Ma (GSWA 206184; this study). The c. 10 Ma between the deposition of the Butchers Gully and Maude Headley Members records turbidity current sedimentation in a deep-marine basin. Few paleocurrent data available indicate a NW-ward paleocurrent, suggesting detritus was either sourced from Pine Creek Orogeny by S-directed transport along NAC margin and/or from Paperbark Supersuite from the west. See p25 for detailed major and trace-element geochemical analysis. 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). Zircon U-Pb geochronological analysis of sample GSWA 206126 (metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 1857+\-3 Ma, interpreted as maximum depositional age. Sample GA 93525128B (metagreywacke) yielded a weighted mean 207Pb*/206Pb* date of 1874+\-3 Ma, interpreted as maximum depositional age. Sample GA 92524896 (coarse-grained subarkosic metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 1858+\-3 Ma, interpreted as maximum depositional age. Sample GSWA 206184 (metasandstone) yielded a weighted mean 207Pb*/206Pb* date of 1834+\-8 Ma, interpreted as maximum depositional age. Lower and Upper Olympio turbidites contain dominantly 1875-1860 Ma detrital zircons, however Upper Olympio also contains  1848-1834 Ma detrital zircons; Hf isotopic data suggest the upper part of Olympio Foramtion may represent deposition into a foreland basin off the NAC.|c. 1856-1834 Ma|Unit of Halls Creek Group.|Includes Butchers Gully Member, Maude Headley Member.|Uppermost unit of Halls Creek Group. Underlain disconformably to unconformably by Biscay Formation. Intruded by Woodward Dolerite and Mount Christine Granite.|Medium to very thick-bedded, lithic and quartzofeldpsathic metasandstone turbidites and metasiltstone hemipalgite.|28-NOV-19
14567|Olympio Formation|71873|5|Briefly described|p426-427|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Depositioanl environment: deep-marine. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.||Unit of Halls Creek Group.||||
14567|Olympio Formation|72437|5|Briefly described|p8, p14, p130|||Four analyses are provided.|c. 1885 Ma||Includes the basal Butchers Gully Member.|Intruded by the Woodward Dolerite.||
14567|Olympio Formation|73089|5|Briefly described|p25-27, p32-33, p36|Orosirian|Orosirian|Lamboo Province, Eastern Zone. Contains a felsic volcanic rock that has an age of 1856 +/- 6 Ma. Dominantly Paleoproterozoic detritus. Paleocurrent indicators have been measured from this unit (north-northeast-south-southwest axis).|c. 1875-1855 Ma|||Underlain by Biscay Formation. May correlate to Killi Killi Formation (Tanami Group).|Metasedimentary rocks.|
14663|Osborne Formation|12758|5|Briefly described|p3 Fig. 3, p22|Late Cretaceous|Early Cretaceous|Basal unit of the Coolyena Group. Geological Province: Perth Basin.||||||07-FEB-08
14663|Osborne Formation|12759|3|Fully described|p38; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Turonian|Aptian|Defined McWhae et al.(1958); redefined here to include 3 Members. Type Section: King Edward Street Bore at AMG Zone 50, 388103m E, 6470027m N (37-133 m).||Basal unit of Coolyena Group.|Includes (this study) Henley Sandstone, Kardinya Shale, and Mirrabooka, Members.|Unconformable on Leederville Formation. Overlain unconformably by Molecap Greensand and Gingin Chalk.||12-MAY-14
14663|Osborne Formation|14227|5|Briefly described|Enclos. 2|||Of Coolyena Group. Presented as Osborne Fm.||||||07-FEB-11
14663|Osborne Formation|23279|6|Mentioned|p31|||||||||
14663|Osborne Formation|23816|4|Described|p248, 250|Cenomanian|Albian|Basal unit of the Coolyena Group. Geological Province: Perth Basin. Underlying unit: Leederville Formation (disconformable). Overlying unit: Kings Park Shale (disconformable). Max. thickness: 97 m.||||||16-DEC-04
14663|Osborne Formation|24058|5|Briefly described|p111 Fig. 4|Cretaceous|Cretaceous|Geological Basin: Perth Basin.||||||
14663|Osborne Formation|24094|5|Briefly described|p274, p278|Cenomanian|Albian|Unconformably overlain by Ascot Formation. Geological Province: Perth Basin||||||16-MAR-05
14663|Osborne Formation|24160|6|Mentioned|p88-90, p94-96|Late Cretaceous|Late Cretaceous|Perth Basin. Mined for shale for use in bricks.||Basal unit in Coolyena Group.||Unconformably overlies Leederville Formation. Is overlain by Molecap Greensand.|Interbedded sandstone, siltstone, shale; characteristically glauconitic.|
14663|Osborne Formation|24410|5|Briefly described|p40|Phanerozoic|Phanerozoic|Sandstone, siltstone, shale. Unconformably overlain by the Guildford Formation. Geological Province: Perth Basin. See also p43 Fig. 9, p143 Fig. 8.||||||24-NOV-09
14663|Osborne Formation|29382|6|Mentioned|Table 10|||||||||
14663|Osborne Formation|29383|6|Mentioned|p14|||See also P16.||||||
14663|Osborne Formation|29693|6|Mentioned|Fig.7|||||||||
14663|Osborne Formation|29721|6|Mentioned|Table 226|||||||||
14663|Osborne Formation|30188|2|Defined|p75|Cretaceous|Cretaceous|Refers McWhae and others(1958).||||||
14663|Osborne Formation|30244|6|Mentioned|p153|||Albian - Cenomanian age||||||
14663|Osborne Formation|30539|6|Mentioned|p24|||Tricoplate grains Albian? - Cenomanian?||||||
14663|Osborne Formation|30939|6|Mentioned|Map legend|Cenomanian|Albian|Cenomanian - Albian||||||
14663|Osborne Formation|31153|4|Described|p110|||Bivalve content & ammonites||||||
14663|Osborne Formation|31238|6|Mentioned|p27|||See also Fig. 12A||||||
14663|Osborne Formation|31562|5|Briefly described|p11|||||||||
14663|Osborne Formation|31568|5|Briefly described|p19|||L-U.Cretaceous. Fig. 2||||||
14663|Osborne Formation|31896|6|Mentioned|p34|||Unconformably o'lain by Guildford Fm.||||||
14663|Osborne Formation|32471|6|Mentioned|p57|||||||||
14663|Osborne Formation|32472|6|Mentioned|p10|||||||||
14663|Osborne Formation|32575|6|Mentioned|p7|||Cretaceous||||||
14663|Osborne Formation|32648|6|Mentioned|p32|||Cret.||||||
14663|Osborne Formation|32714|6|Mentioned|Fig.2|||||||||
14663|Osborne Formation|32747|6|Mentioned|p365|||Comparison of sediments||||||
14663|Osborne Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
14663|Osborne Formation|33015|6|Mentioned|p13|||||||||
14663|Osborne Formation|33044|4|Described|p40|||See also map 3 & diag. 16,17,18.||||||
14663|Osborne Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
14663|Osborne Formation|33386|6|Mentioned|Fig.7|||||||||
14663|Osborne Formation|34112|6|Mentioned|p3|||||||||
14663|Osborne Formation|34343|6|Mentioned|p96|||||||||
14663|Osborne Formation|34413|6|Mentioned|p13|||Albian - Cenomanian||||||
14663|Osborne Formation|34414|6|Mentioned|p53|||Albian - Cenomanian||||||
14663|Osborne Formation|34841|6|Mentioned|Fig.2|||||||||
14663|Osborne Formation|35057|5|Briefly described|p301|||||||||
14663|Osborne Formation|35058|6|Mentioned|p65|||||||||
14663|Osborne Formation|35282|6|Mentioned|Fig.6|||||||||
14663|Osborne Formation|35638|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
14663|Osborne Formation|35968|5|Briefly described|p64|||See also Fig.8.||||||
14663|Osborne Formation|35970|6|Mentioned|p77|||See also Table 12.||||||
14663|Osborne Formation|35973|6|Mentioned|p93|||||||||
14663|Osborne Formation|36257|6|Mentioned|Table 2.1|||||||||
14663|Osborne Formation|36265|5|Briefly described|Fig.3.26|Late Cretaceous|Early Cretaceous|Geological province: Perth Basin.||||||04-MAR-08
14663|Osborne Formation|36293|2|Defined|p178|Cenomanian|Albian|Albian-Cenomanian||||||
14663|Osborne Formation|36552|6|Mentioned|p17|||See also P47.||||||
14663|Osborne Formation|36890|3|Fully described|p250|||||||||
14663|Osborne Formation|37104|6|Mentioned|Fig.3|||||||||
14663|Osborne Formation|37360|5|Briefly described|Fig.13|||See also Fig.3.||||||
14663|Osborne Formation|38221|6|Mentioned|Fig.4|||Perth Basin.||||||
14663|Osborne Formation|38778|4|Described|p19|||||||||
14663|Osborne Formation|39156|4|Described|p22|||||||||
14663|Osborne Formation|39211|6|Mentioned|p61|||See also P62,66||||||
14663|Osborne Formation|39829|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14663|Osborne Formation|40348|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
14663|Osborne Formation|40349|5|Briefly described|p17|||||||||
14663|Osborne Formation|40395|6|Mentioned|p334|||||||||
14663|Osborne Formation|40902|6|Mentioned|p55|||||||||
14663|Osborne Formation|41341|6|Mentioned|p51|||||||||
14663|Osborne Formation|41634|6|Mentioned|p42|||||||||
14663|Osborne Formation|41783|4|Described|p41|||||||||
14663|Osborne Formation|41986|6|Mentioned|p34|||||||||
14663|Osborne Formation|41989|4|Described|p114|||||||||
14663|Osborne Formation|42001|6|Mentioned|Fig.2 P79|||||||||
14663|Osborne Formation|42194|5|Briefly described|p5|||||||||
14663|Osborne Formation|43062|5|Briefly described|Table 2,p18|||Coolyena Group||||||
14663|Osborne Formation|43252|5|Briefly described|p163|||||||||
14663|Osborne Formation|43347|6|Mentioned|9|||||||||
14663|Osborne Formation|44144|4|Described|p503 Tb.4-21, p517|Turonian|Albian|Type Section: King Edward Street bore; 31o54'S 115o49'E; 37-133m. 200m thick marine shelf deposits.||Coolyena Group||Overlies Leederville Formation disconformably. Overlain by Molecap Greensand conformably.|Interbedded sandstone, siltstone, shale and claystone; characteristically glauconitic; argillaceous sediments usually dark grey or black.|
14663|Osborne Formation|61811|5|Briefly described|p3 Fig.2, pp54-57, p65.|Albian|Aptian|Northern Perth Basin. Type section details in Appendix 1.||Unit in Coolyena Group.||Unconformably overlies Warnbro Group. Is overlain by Molecap Greensand.|Glauconitic sandstone, siltstone and claystone.|
14663|Osborne Formation|63745|5|Briefly described|p66|Cretaceous|Cretaceous|||||||07-FEB-11
14663|Osborne Formation|64580|4|Described|map legend||Late Cretaceous|Of Coolyena Group. Interbedded sandstone, siltstone, shale and claystone; characteristically glauconitic.||||||09-DEC-08
14663|Osborne Formation|64635|5|Briefly described|p4 Fig.3 |Albian|Aptian|||Unit in Coolyena Group.||||
14663|Osborne Formation|67115|6|Mentioned|p64, p65 Fig.3 |Cretaceous|Cretaceous|Lithology and trace elements detailed.|||Kardinya Shale Member, Mirrabooka Member.|Overlies the Leederville Formation; underlies the Molecap Greensand.||
14663|Osborne Formation|67340|6|Mentioned|p6|Late Cretaceous|Early Cretaceous|Northern Perth Basin.||Coolyena Group.||||
14663|Osborne Formation|67925|5|Briefly described|Ch2 p10 fig 4|Cenomanian|Aptian|||||Unconformably overlies the Leederville Formation.||
14663|Osborne Formation|68254|5|Briefly described|p1036 Fig.2, p1040 Tb.3, p1046 Tb.4|Cretaceous|Cretaceous||||Includes Mirrabooka Member, Kardinya Shale Member, and Henley Sandstone Member.|||
14663|Osborne Formation|69081|5|Briefly described|p737 Fig.1|Late Cretaceous|Early Cretaceous|Presented as Osborne Fm in figure. Geol. Prov: Perth Basin.||Coolyena Group||Unconformably overlies Leederville Formation.||23-JUL-15
14663|Osborne Formation|69182|6|Mentioned|Ch2 p3, Ch2 p9, Ch2 p55, Ch2 p57|||Perth Basin.||Coolyena Group||Overlies the Dandaragan Sandstone. Overlain by the Molecap Greensand.||
14663|Osborne Formation|69297|6|Mentioned|p175, p189|Turonian|Aptian|Vlaming Sub-basin, South Perth Basin.||Coolyena Group||Overlies the Leederville Formation. Overlain by the Molecap Greensand.||
14663|Osborne Formation|70097|5|Briefly described|p20 Fig.4|Albian|Albian|Northern Perth Basin. Dandaragan Trough.||Coolyena Group||Overlies Dandaragan Sandstone. Is overlain by Molecap Greensand.|Limestone.|12-SEP-17
14663|Osborne Formation|70099|5|Briefly described|Fig.4; p6|Cenomanian|Aptian|||Coolyena Group.|Henley Sandstone Member, Kardinya Shale Member.|Overlies Leederville Formation (Warnbro Group). Is overlain by Molecap Greensand.||
14663|Osborne Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, claystone, greensand|
14663|Osborne Formation|71377|5|Briefly described|p9|||Perth Basin.||Coolyena Group||Unconformably overlies the Leederville Formation.||
14663|Osborne Formation|71790|6|Mentioned|p102|||Palynology p. 102.||||||
14663|Osborne Formation|72034|5|Briefly described|500k_interpgeop16_lut|Turonian|Albian|Perth Basin.  Age from biostratigraphy.||Coolyena Group|||Interbedded sandstone, siltstone, shale, and claystone; characteristically glauconitic.|
14667|Oscar Range Group|22716|6|Mentioned|table4, p239|Cryogenian|Cryogenian|Age: ~830 Ma shown in correlation chart. Thought to be part of supersequence 1 of Centralian Superbasin||||||17-OCT-12
14667|Oscar Range Group|42710|5|Briefly described|map legend|Proterozoic|Proterozoic|Variation on Oscar Range Succession.  Not related to Oscar Formation.|<1800, >670 Ma|||||17-OCT-12
14667|Oscar Range Group|42811|3|Fully described|p27|Neoproterozoic|Mesoproterozoic|Stratigraphic relationships difficult to establish due to disruption by shear zones.|No reliable isotopic data. Post Yampi Orogeny.||Includes Mount Wilson Formation, Christopher Formation, Le Lievre Formation, Ellendale Formation, Linesman Formation. Mount Wilson, Christopher and Le Lievre may be parts of same unit.|Probably equivalent to Glidden Group, Carr Boyd Group, Osmond Range succession.||17-OCT-12
14667|Oscar Range Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
14667|Oscar Range Group|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
14667|Oscar Range Group|43819|6|Mentioned|p31|Neoproterozoic|Mesoproterozoic|||||||
14667|Oscar Range Group|64580|4|Described|map legend||Neoproterozoic|Sandstone, siltstone, shale, conglomerate, and altered mafic igneous rock.||||||09-DEC-08
14667|Oscar Range Group|69099|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic||||||Sandstone, siltstone, shale, conglomerate, and altered mafic igneous rock|04-AUG-15
14667|Oscar Range Group|69165|4|Described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Sandstone, siltstone, shale, conglomerate and altered mafic igneous rock.|
14667|Oscar Range Group|69437|6|Mentioned|p22:1|||Centralian A Superbasin (Centralian Superbasin of Walter et al., 1995).||||||12-JUL-16
14667|Oscar Range Group|69634|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic||||||Sandstone, siltstone, shale, conglomerate, and altered mafic igneous rock|
14667|Oscar Range Group|70154|4|Described|500k_interpgeop14_lut.csv|Ediacaran|Ediacaran||541-635 Ma||||Sandstone, siltstone, shale, conglomerate and altered mafic igneous rock.|
14667|Oscar Range Group|71267|5|Briefly described|1M_geologyp12_lut.csv|Neoproterozoic|Neoproterozoic|Of Oscar Range Sub-basin. Louisa Basin, Centralian Superbasin. Events: King Leopold Orogeny (670-510 Ma). See 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-541 Ma (inferred)||Includes Christopher Formation, Ellendale Formation, Le Lievre Formation, Linesman Formation, Mount Wilson Sandstone.||Sandstone, siltstone, shale, conglomerate, and altered mafic igneous rock|
14667|Oscar Range Group|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Oscar Range Sub-basin, Louisa Basin.|||||Sandstone, siltstone, shale, conglomerate, and altered mafic igneous rock.|
14667|Oscar Range Group|73086|6|Mentioned|p4 Fig.4|||||||||
14669|Osprey Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5|Middle Triassic|Middle Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
14669|Osprey Formation|7142|6|Mentioned|p350 Fig.4.|Middle Triassic|Early Triassic|Browse Basin.||||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|13194|6|Mentioned|p386 Tb. 4-16|Anisian|Anisian|Type Section: Osprey 1 well (1318-1834m). Up to 516m thick shallow marine deposits.||Sahul Group||Overlies Mount Goodwin Formation (conformably). Overlain by Pollard Formation.|Interbedded shale and sandstone; minor carbonate.|
14669|Osprey Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
14669|Osprey Formation|13242|5|Briefly described|p225|||Unconformably overlies Upper Mount Goodwin Formation in the west. Includes sandstones.||||||07-FEB-11
14669|Osprey Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Triassic|Late Permian|Bonaparte Basin. Unit of Sahul Group. Overlies Mount Goodwin Formation and underlies Pollard Formation. Equivalent to Erskine Sandstone of onshore Canning Basin.||161||||28-OCT-14
14669|Osprey Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Middle Triassic|Of the Sahul Group.||||||01-MAR-10
14669|Osprey Formation|23378|6|Mentioned|p180 Fig.2|Middle Triassic|Early Triassic|Of the Sahul Group.  In the Vulcan Sub-basin.||||||21-NOV-06
14669|Osprey Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
14669|Osprey Formation|24207|5|Briefly described|p209 Fig. 5|Middle Triassic|Middle Triassic|||||||01-MAR-10
14669|Osprey Formation|41532|2|Defined|p302|Middle Triassic|Early Triassic|||||||
14669|Osprey Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
14669|Osprey Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
14669|Osprey Formation|42442|2|Defined|p21|Anisian|Scythian|NT and WA. Age: Early to Middle Triassic (late Scythian to Anisian).||||||14-APR-08
14669|Osprey Formation|43826|6|Mentioned|Fig.2,p163||Middle Triassic|||||||01-MAR-10
14669|Osprey Formation|60634|6|Mentioned|p1168 Fig.3. |Middle Triassic|Middle Triassic|||Unit in Sahul Group.||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|61550|6|Mentioned|p495 Fig.2.|||||Unit in Sahul Group.||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||09-NOV-12
14669|Osprey Formation|63358|5|Briefly described|p4 Fig. 1.3|Anisian|nammalian|||||||01-MAR-10
14669|Osprey Formation|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine sediments.||||Overlies Mount Goodwin Formation. Is overlain by Pollard Formation.||
14669|Osprey Formation|66124|5|Briefly described|p171 Fig.2|Anisian|Anisian|Ashmore Platform (East). Marine. Underlies Pollard Formation and overlies Mount Goodwin Formation.||||||
14669|Osprey Formation|66187|5|Briefly described|p413 Fig.2|Middle Triassic|Early Triassic|Sahul Group. Underlies the Pollard Formation, overlies the Mount Goodwin Formation. Mount Ashmore Dome.||||||
14669|Osprey Formation|67370|6|Mentioned|p313 Fig.2, p323 Fig.14. |Triassic|Triassic|||||Overlies Mount Goodwin Subgroup. Is overlain by Crane Formation.||
14669|Osprey Formation|68223|6|Mentioned|p178 Fig.3|Ladian|Scythian|||||||
14669|Osprey Formation|69297|6|Mentioned|p305|Ladinian|Anisian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Sahul Group||Overlies the Kinmore Group. Overlain by the Pollard Formation.|Siltstone and mudstone.|
14669|Osprey Formation|69452|5|Briefly described|p36:15, 21|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||Equivalent to lower part of Cape Londonderry Formation.||12-JUL-16
14669|Osprey Formation|69653|6|Mentioned|p10|Middle Triassic|Middle Triassic|Petrel Sub-basin.||Troughton Group.||Equivalent to Lower Cape Londonderry Formation.||
14669|Osprey Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||||
14669|Osprey Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Anisian|Anisian|See also Regional geology: Figs.6-7. Vulcan: Fig.2. Equivalent to the lower part of Cape Londonderry Formation.||Sahul Group.||Overlies Fishburn Formation (Mount Goodwin Subgroup). Is overlain by Pollard Formation.||12-JUL-16
14669|Osprey Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Ladinian|Anisian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins, Browse Basin.||Sahul Group.||Overlies Kinmore Group. Is overlain by Pollard Formation.||12-JUL-16
14669|Osprey Formation|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Bonaparte Basin.||||Overlies the Mount Goodwin Subgroup. Overlain by the Sahul Group.|Mudstone.|
14749|Paddington Dolerite|41066|5|Briefly described|p32|||||||||
14749|Paddington Dolerite|41379|6|Mentioned|p44|||||||||
14749|Paddington Dolerite|42289|5|Briefly described|p30|||||||||
14749|Paddington Dolerite|63463|6|Mentioned|p587|||Leucoxene-bearing dolerite sill.||||||
14753|Paddy Market Formation|22642|5|Briefly described|485|||Geol province Pilbara Craton.||||||22-OCT-08
14753|Paddy Market Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Soanesville Subgroup, Pilbara Craton.||||||07-NOV-08
14753|Paddy Market Formation|23755|4|Described|p44|Archean|Archean|See also page 17 table 1. Of Gorge Creek Group.||||||07-NOV-08
14753|Paddy Market Formation|23783|5|Briefly described|p17|||Of Gorge Creek Group.||||||
14753|Paddy Market 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
14753|Paddy Market Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Gorge Creek Group.  Geological Province: Pilbara Craton||||||07-NOV-08
14753|Paddy Market Formation|24184|5|Briefly described|p702, p699 Fig.3|Archean|Archean|Parent: George Creek Group. Overlying Unit: Honeyeater Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
14753|Paddy Market Formation|24531|5|Briefly described|p20|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group).  Ferruginized and silicified grey shales and BIF.  Conformably overlies the Corboy Formation. See also p5 Table 1. Geological Province: Pilbara Craton.||||||07-NOV-08
14753|Paddy Market Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of Soanesville Subgroup (Gorge Creek Group).||||||07-NOV-08
14753|Paddy Market Formation|24550|5|Briefly described|p31 Tb. 3.1|||Of the Gorge Creek Group. Shale, chert. Geological Province: Pilbara Craton.||||||07-FEB-11
14753|Paddy Market Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). Fe-shale; locally silicified to grey and white chert.||||||07-FEB-11
14753|Paddy Market Formation|31853|2|Defined|p62|Archean|Archean|||||||07-NOV-08
14753|Paddy Market Formation|37373|4|Described|p79|||||||||
14753|Paddy Market Formation|39426|6|Mentioned|Table 1|||||||||
14753|Paddy Market Formation|39444|6|Mentioned|Table 1|||||||||
14753|Paddy Market Formation|41252|6|Mentioned|p49|||||||||
14753|Paddy Market Formation|42231|6|Mentioned|p333|||||||||
14753|Paddy Market Formation|43595|6|Mentioned|p217|||||||||
14753|Paddy Market Formation|44150|6|Mentioned|p135|||Of Lipple (1975).||||Equivalent to Cleaverville Formation.||
14753|Paddy Market Formation|50189|6|Mentioned|p18|||Also called Cleaverville Formation historically.||||||
14753|Paddy Market Formation|60429|6|Mentioned|p18|||||||||07-FEB-11
14753|Paddy Market Formation|61253|5|Briefly described|p51|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
14753|Paddy Market Formation|61266|5|Briefly described|p58 Tb.1, p60|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). Intruded by the Dalton Suite. Fe-shale; locally silicified to grey and white chert. Geological Province: Pilbara Craton.||||||07-NOV-08
14753|Paddy Market Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Gorge Creek Group.||||||07-NOV-08
14753|Paddy Market Formation|63441|5|Briefly described|p4 Tb. 1, p22|Archean|Archean|Of the Soanesville Group (Pilbara Supergroup). Thickness: 1040m in NORTH SHAW area. Predominantly shale. Conformably overlies Corboy Formation; conformably (or disconformably?) overlain by Honeyeater Basalt. Geological province: Pilbara Craton.||||||07-FEB-11
14753|Paddy Market Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Soanesville Group. Underlain by Corboy Formation, overlain by Honeyeater Basalt. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
14753|Paddy Market Formation|64328|5|Briefly described|p56 Tb. 1, p58|||Shale, banded iron formation.||||||07-FEB-11
14753|Paddy Market Formation|64405|5|Briefly described|p4 Fig. 3|Archean|Archean|Name inferred from Paddy Market only in Figure 3. Of the Soanesville Group (De Grey Supergroup). Age: 3190Ma. Sedimentary.||||||07-FEB-11
14753|Paddy Market Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of George Creek Group. Geological Province: Pilbara Craton. Thinly bedded banded iron-formation interbedded with ferruginous chert; wealky metamorphosed.||||||07-FEB-11
14753|Paddy Market Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Soanesville Subgroup. Under Lalla Rookh Sandstone; over Corboy Formation. Cherty banded iron-formation; minor ferruginous shale. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
14753|Paddy Market Formation|65008|4|Described|p7, p8 Fig.5, p14, p41|Mesoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Age constrained by the parent Gorge Creek Group.|3235-2950 Ma|Of the Gorge Creek Group||Unconformably overlain by the Coondamar Formation? Conformably underlain by the Corboy Formation.|Consists of thinly bedded iron-formation interbedded with ferruginous chert. The iron-formation comprises white and black laminae of ferruginous shale, and variably ferruginised or silicified chert.|
14753|Paddy Market Formation|65757|5|Briefly described|p83 Fig.3|Mesoarchean|Paleoarchean|in the Soanesville Group||||||
14753|Paddy Market Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Soanesville Group. Banded iron-formation, chert, siliciclastic sedimentary rocks, and local felsic volcanic rocks; metamorphosed.||||||
14753|Paddy Market Formation|66118|5|Briefly described|p149 Fig.3|||Pilbara Craton. East Pilbara Terrane.||||Dalton Suite intrudes and overlies Paddy Market Formation in Soanesville greenstone belt. Overlies Corboy Formation.||
14753|Paddy Market Formation|66217|6|Mentioned|p41.|||Previously, included rocks now attributed to Cleaverville Formation.||Unit in Gorge Creek Group.||||
14753|Paddy Market Formation|66745|5|Briefly described|p53 Fig.3.|Mesoarchean|Mesoarchean|||Unit in Soanesville Group.||Overlies Corboy Formation. Is overlain by Honeyeater Basalt.|Shale.|
14753|Paddy Market Formation|67130|5|Briefly described|p16|||||Soanesville Group||Overlies Corboy Sandstone, overlain by Honeyeater Basalt|Shale and siltstone|
14753|Paddy Market Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Soanesville Group.||||
14753|Paddy Market Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane, Soanesville Basin, rift-related successions.||Soanesville Group||||
14753|Paddy Market Formation|67668|6|Mentioned|Fig. 2; p. 154||Mesoarchean|East Pilbara Terrane, Pilbara Craton.||Soanesville Group||Underlies the Honeyeater Basalt, overlies the Corboy Formation.|Clastic sediments.|
14753|Paddy Market Formation|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton.|< 3190 Ma|Of the Soanesville Group|||Cherty banded iron-formation and chert, thinly-bedded and partly jaspilitic, minor ferruginous shale; red-weathered, ferruginized shale, grey-green shale, and siltstone; all metamorphosed.|
14753|Paddy Market Formation|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Soanesville Basin. Mapped as 3 separate facies.||Of the Soanesville Group.|||Iron-formation; cherty banded iron-formation and chert, thinly bedded and partly jaspilitic, minor ferruginous shale; silicified shale, grey- and white-layered secondary chert; all metamorphosed.|30-APR-14
14753|Paddy Market Formation|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Pilbara Craton. Mapped as 5 unnamed sub-units.||Of the Soanesville Group.|||Iron-formation; banded iron-formation and chert, minor ferruginous shale; red-weathered, ferruginised shale, grey-green shale, and siltstone; silicified shale, grey and white layered secondary chert; massive to spherulitic dacite; all metamorphosed.|02-MAY-14
14753|Paddy Market Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Soanesville Group|||Meta-iron formation, cherty banded iron formation and chert; thinly bedded and partly jaspilitic. Ferruginized shale, siltstone and massive to spherulitic dacite.|
14753|Paddy Market Formation|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv||Mesoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Unit of Gorge Creek Group.||||
14753|Paddy Market Formation|69301|5|Briefly described|p5 Fig.3, p9 Tb.1, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Soanesville Basin. Rift-related successions.||Soanesville Group||||
14753|Paddy Market 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.|||Cherty banded iron-formation and chert; metamorphosed; massive to spherulitic dacite; metamorphosed; ferruginised shale and siltstone, silicified shale, layered chert, metamorphosed.|
14753|Paddy Market Formation|69616|5|Briefly described|p159, p161-164, p166, p169-178|Archean|Archean|See also p180-181, p184. Thickness to 400m. Characterised by abundant folds from deformation. Displays abundant slump folds and bedding-parallel pinch and swell structures. Displacement up to tens of metres across both normal and reverse faults. Hydrothermal alteration and mineralisation discussed.||Unit in Soanesville Group.||Overlies Corboy Formation. Is overlain by Honeyeater Basalt.|Millimetre- and centimetre-scale interbedded siltstone and chert layers with minor sandstone.|
14753|Paddy Market Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Soanesville Group.||||
14753|Paddy Market Formation|70775|5|Briefly described|p12|||East Pilbara.||Soanesville Group||Overlies the Corboy Formation. Overlain by the Honeyeater Basalt.||
14753|Paddy Market Formation|71041|5|Briefly described|p43|Mesoarchean|Mesoarchean|East Pilbara Terrane. Deposited under mid to outer fan and basin-plain settings.|3190 Ma||||Includes banded iron formation.|10-NOV-17
14753|Paddy Market Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Paleoarchean|Soanesville Basin.||Soanesville Group|||Banded iron-formation, chert, siliciclastic sedimentary rocks, and local felsic volcanic rocks; metamorphosed.|
14753|Paddy Market Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Soanesville Group.||Overlain by Honeyeater Basalt. Underlain by Corboy Formation.||
14753|Paddy Market Formation|72668|5|Briefly described|p4-6|||East Pilbara Terrane.||Soanesville Group||Overlies the Corboy Formation. Overlain by the Honeyeater Basalt.|Shale and siltstone.|
14753|Paddy Market Formation|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Soanesville Group.||Overlies Corboy Formation. Is overlain by Honeyeater Basalt.||
14772|Padthureena Serpentinite|32190|6|Mentioned|p171|||||||||
14796|Pallinup Formation|23331|3|Fully described|1088||Late Eocene|Proposed name change for Pallinup Siltstone.||||||10-SEP-09
14796|Pallinup Formation|23533|5|Briefly described|p561|Late Eocene|Late Eocene|Of Plantagenet Group. Underlying unit Werrilup Formation. Geological Province: Bremer Basin.||||||
14796|Pallinup Formation|23768|5|Briefly described|p28 Fig.5|Late Eocene|Late Eocene|Geological Province: Bremer Basin.||||||30-MAR-05
14796|Pallinup Formation|24397|4|Described|p242|Eocene|Eocene|Direct equivalent of Khasta Formation in South Australia.  Now includes Princess Royal Member and Pallinup Limestone.  Geological Province: Eucla Basin.||||||
14796|Pallinup Formation|24557|5|Briefly described|p958, p959 Fig.2, p960 Fig.3|Late Eocene|Late Eocene|Embayment-archipelago sediments: comprises four informal units plus uppermost Fitzgerald Member; sponge-rich facies, spiculite and spongolite shoreface deposits, sub-shoreface muddy spiculte and spiculitic mudstone. Geological Province: Bremer Basin.||||||11-JAN-05
14796|Pallinup Formation|32311|5|Briefly described|p7|||Stratigraphic table.||||||21-OCT-08
14796|Pallinup Formation|32648|6|Mentioned|p32|||Tertiary||||||
14796|Pallinup Formation|41043|6|Mentioned|p86|||||||||
14796|Pallinup Formation|42473|6|Mentioned|p41|||See also Pallinup Siltstone p.6.||||||
14796|Pallinup Formation|61273|5|Briefly described|p85|Eocene|Eocene|Contains spongolite - a pale brown porous rock composed of siliceous, fossil sponge spicules. Has excellent insulating properties and has been used as a lightweight building material.  Geological Province: Bremer Basin.||||||
14796|Pallinup Formation|62069|5|Briefly described|p104|Late Eocene|Late Eocene|Supersedes Pallinup Siltstone.  New species of Stirpulina (bivalve) found in cream, pink and yellow-brown, siliceous, spicular siltstone of the pallinup Formation near Esperance. Geological Province: Bremer Basin.||||||27-APR-06
14796|Pallinup Formation|64340|5|Briefly described|p26 Tb. 5, p28|Late Eocene|Late Eocene|Of Eundyine Group. Includes Princess Royal Formation.||||||
14796|Pallinup Formation|64580|4|Described|map legend|Eocene|Eocene|Of Plantagenet Group. Siltstone, spongolite; silty and spicule-rich sandstone.||||||21-OCT-08
14796|Pallinup Formation|65194|5|Briefly described|p138 Fig.4.38|Late Eocene|Middle Eocene|Shown as including Princess Royal Spongolite as Princess Royal Member (Clarke et al. 2003).||||||
14796|Pallinup Formation|65260|6|Mentioned|p26, p27 Fig.20|Late Eocene|Late Eocene|Cowan Palaeochannel. Most likely correlates with undivided Eundynie Group. In stratigraphy proposed by Clarke (2003), includes Princess Royal Member.||||||
14796|Pallinup Formation|65264|5|Briefly described|p28, p43 Appdx. 1|Late Eocene|Late Eocene|Of the Eundynie Group. Geological province: Eucla Basin. Conglomerate.||||||19-JAN-15
14796|Pallinup Formation|65891|6|Mentioned|p221 Fig.5. |||Bremer and West Eucla Basins. Age Priabonian.||||||
14796|Pallinup Formation|68811|6|Mentioned|p156 app 1|||See also Pallinup Sandstone and Siltstone units.||||||
14796|Pallinup Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Eocene|Eocene|||Plantagenet Group|Includes Princess Royal Member.||Sandstone, quartz-rich and poorly sorted, with spongolitic and calcareous varieties; includes subordinate gravel, conglomerate, and siltstone.|07-AUG-15
14796|Pallinup Formation|69412|6|Mentioned|p3 Fig.2|Eocene|Eocene|Ravensthorpe-Hopetoun area, Yilgarn Craton.||||||
14796|Pallinup Formation|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Late Eocene|Late Eocene|Eucla Basin. Contains potential sealing lithologies. Also referred to as the Pallinup Siltstone on p9.||Plantagenet Group|Includes the Fitzgerald and Princess Royal Members.|Overlies the Werrilup Formation.|Claystones, siltstones, sandstones and spongolite facies.|
14796|Pallinup Formation|70153|5|Briefly described|100k_geologyp10_lut.csv|Eocene|Eocene|Eucla Basin.||Plantagenet Group|||Sandstone, quartz-rich and poorly sorted, with spongolitic and calcareous varieties; includes subordinate gravel, conglomerate (fluvioglacial/glacigene), and siltstone|
14796|Pallinup Formation|70802|5|Briefly described|GEOL_LUT_CSV files|Eocene|Eocene|Of Esperance Shelf, Eucla Basin. Events: Timorese Collision. See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv.||Unit of Plantagenet Group.|||Sandstone, quartz-rich and poorly sorted, with spongolitic and calcareous varieties; includes subordinate gravel, conglomerate, and siltstone|
14796|Pallinup Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone, claystone|
14796|Pallinup Formation|71270|4|Described|GEOL_LUT_CSV files|Eocene|Eocene|Of Eucla Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Plantagenet Group.|Includes Princess Royal Member.||Sandstone, quartz-rich and poorly sorted, with spongolitic and calcareous varieties; includes subordinate gravel, conglomerate, and siltstone|
14796|Pallinup Formation|72034|5|Briefly described|500k_interpgeop16_lut|Eocene|Bartonian|Eucla Basin. Age from biostratigraphy.||Plantagenet Group|||Siltstone, spongolite; silty and spicule-rich sandstone; lesser fossiliferous limestone.|
14813|Pander Greensand|6943|6|Mentioned|p604.|||Bonaparte Basin. Contains Teriodontus conodonts.||||||
14813|Pander Greensand|13194|4|Described|p394 Tb. 4-16; p382, 399 figs 4-59,-63|Ordovician|Cambrian|Type Section: Pander Ridge 15o28'S 128o41'S. 40-120m thick shallow marine deposits.||Carlton Group||Overlies Clark Sandstone (conformably).|Glauconitic quartz sandstone.|
14813|Pander Greensand|14228|6|Mentioned|p6 fig3|||Southern Bonaparte Basin.||||Overlies Clark Sandstone.||
14813|Pander Greensand|24390|5|Briefly described|p2 Fig. 2||Cambrian|Geological Province: Bonaparte Basin. Of the Carlton Group.||||||
14813|Pander Greensand|30598|6|Mentioned|p51|||||||||
14813|Pander Greensand|31396|6|Mentioned|p1183|||||||||
14813|Pander Greensand|31572|6|Mentioned|p22|||L.Ord. Correlation chart 1||||||
14813|Pander Greensand|32109|6|Mentioned|Table 1|||Lower Ordovician||||||
14813|Pander Greensand|32648|6|Mentioned|p32|||Arenig||||||
14813|Pander Greensand|32664|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|Briefly described in notes||||||
14813|Pander Greensand|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969)||||||
14813|Pander Greensand|33738|6|Mentioned|p44|||||||||
14813|Pander Greensand|34287|6|Mentioned|p74|||||||||
14813|Pander Greensand|36257|6|Mentioned|Table 2.1|||||||||
14813|Pander Greensand|36551|6|Mentioned|Table 16|||||||||
14813|Pander Greensand|36890|3|Fully described|p375|||||||||
14813|Pander Greensand|38444|6|Mentioned|p301|||||||||
14813|Pander Greensand|40127|6|Mentioned|p8|||||||||
14813|Pander Greensand|40136|5|Briefly described|p36|||||||||
14813|Pander Greensand|40993|6|Mentioned|Fig.1|||||||||
14813|Pander Greensand|41459|6|Mentioned|Fig.2|||||||||
14813|Pander Greensand|41690|6|Mentioned|Fig.2|||||||||
14813|Pander Greensand|41731|6|Mentioned|Fig.3|||||||||
14813|Pander Greensand|41864|3|Fully described|p45|||||||||
14813|Pander Greensand|41865|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
14813|Pander Greensand|43236|5|Briefly described|p13|Tremadoc||Bonaparte Basin||||||
14813|Pander Greensand|43661|6|Mentioned|Fig.3|||||||||
14813|Pander Greensand|45038|14|Not recorded|Fig.2||Ordovician|||||||
14813|Pander Greensand|45039|6|Mentioned|Fig.2|||Lower Ordovician||||||
14813|Pander Greensand|45050|6|Mentioned|p42|||Lower Ordovician||||||
14813|Pander Greensand|45058|5|Briefly described|p7|||||||||
14813|Pander Greensand|48886|4|Described|p.49||Early Ordovician|See also Figs & Plates, App.2, p.66. Lower Ordovician.||||||
14813|Pander Greensand|49637|5|Briefly described|Fig. 6|Early Ordovician|Early Ordovician|Of the Carlton Group. Age: ~500Ma. Geological Province: Bonaparte Basin.||||||07-FEB-11
14813|Pander Greensand|50085|5|Briefly described|p2 Fig. 2|Early Ordovician|Late Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||10-APR-08
14813|Pander Greensand|61023|5|Briefly described|p2 Fig. 2|Ordovician|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||10-APR-08
14813|Pander Greensand|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
14813|Pander Greensand|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
14813|Pander Greensand|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
14813|Pander Greensand|69437|5|Briefly described|p22:10|Early Ordovician|Furongian|Bonaparte Basin, Centralian B Superbasin.||Carlton Group.||Overlies Clark Sandstone.||12-JUL-16
14813|Pander Greensand|69452|5|Briefly described|p36:5|Early Ordovician|Furongian|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Conformably overlies Clark Sandstone.||12-JUL-16
14813|Pander Greensand|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
14813|Pander Greensand|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian|||Carlton Group||Overlies Clark Sandstone||
14813|Pander Greensand|71146|5|Briefly described|p6|Early Ordovician|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Clark Sandstone.|Sandstone.|
14834|Panorama Formation|22615|5|Briefly described|p 7||Archean|Age: 3459 +9 /- 4Ma.||||||07-NOV-08
14834|Panorama Formation|23206|5|Briefly described|p1256, Fig.1||Archean|Age: 3.46Ga. of Warrawoona Group, Pilbara.||||||07-NOV-08
14834|Panorama Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup, Pilbara Craton||||||07-NOV-08
14834|Panorama Formation|23755|4|Described|p23|Archean|Archean|Age: 3458-3454 Ma. See also page 17 table 1. Of Warrawoona Group.||||||07-NOV-08
14834|Panorama Formation|23780|5|Briefly described|p111|Archean|Archean|Age: ~3433-3451 Ma. Of the Warrawoona Group.||||||07-NOV-08
14834|Panorama Formation|23783|4|Described|p14|Archean|Archean|Of Salgash Group.  See also p73.||||||07-NOV-08
14834|Panorama Formation|23807|5|Briefly described|p111|Archean|Archean|Of Salgash Group.  Age: 3458+/-2Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|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
14834|Panorama Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Salgash Subgroup (Warrawoona Group).  Felsic lavas, tuffs, agglomerate, chert, and tuffaceous sedimentary rocks. Max. thickness: 1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Warrawoona Group.  Geological Province: Pilbara Craton||||||07-NOV-08
14834|Panorama Formation|24182|5|Briefly described|p93|||Age: 3471+/-5 - 3458 +/- 1.9 Ma.  Underlies Strelley Pool Chert. Geological Province: Pilbara Craton.||||||24-JUL-07
14834|Panorama Formation|24184|5|Briefly described|p699 Fig.3, p701|Archean|Archean|Parent: Salgash Group. Overlying Unit: Strelley Pool Chert. Underlying Unit: Apex Basalt. Geological Province: Pilbara Craton. Max Thickness: 1.5km. Age: ca.3459-3426Ma. Overlies Duffer Formation where Apex Basalt is missing||||||07-NOV-08
14834|Panorama Formation|24185|5|Briefly described|p734, p751|Archean|Archean|Age: ca. 3458-3428 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|24531|4|Described|p17|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Mainly composed of felsic volcaniclastic rocks, subordinate felsic lavas and chert, and beds of quartzite.  Age: c.3458-3426Ma.    Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Age: c.3434Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Felsic volcanics, tuffaceous sandstones.  Age: 3459-3434Ma. Max. thickness: 1.5km. Geological Province: Pilbara Craton.||||||07-FEB-11
14834|Panorama Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Felsic lavas, tuffs and tuffaceous sandstone. Overlies Strelley Pool Chert (??); overlain by Euro Basalt. Age: 3458+/-2Ma and ca.3415+/-8Ma. Max. thickness: 1000m. See also p129-130.||||||07-FEB-11
14834|Panorama Formation|31309|6|Mentioned|Table 8|||refs Lipple 1975||||||
14834|Panorama Formation|31853|2|Defined|p61|Archean|Archean|||||||07-NOV-08
14834|Panorama Formation|37373|4|Described|p79|||||||||
14834|Panorama Formation|38498|5|Briefly described|Table 1|||||||||
14834|Panorama Formation|38544|6|Mentioned|Fig.1|||||||||
14834|Panorama Formation|39444|6|Mentioned|Table 1|||||||||
14834|Panorama Formation|39672|6|Mentioned|p238|||||||||
14834|Panorama Formation|39697|3|Fully described|p95|||||||||
14834|Panorama Formation|40596|6|Mentioned|p65|||||||||
14834|Panorama Formation|41028|6|Mentioned|p227|||||||||
14834|Panorama Formation|41767|5|Briefly described|p45|||See also p46.||||||24-JUL-07
14834|Panorama Formation|41851|5|Briefly described|p823|||||||||
14834|Panorama Formation|43595|6|Mentioned|Table 2-28,p214|||||||||
14834|Panorama Formation|43698|6|Mentioned|p26|||||||||
14834|Panorama Formation|43769|6|Mentioned|Fig.3,p858|||||||||
14834|Panorama Formation|44150|4|Described|p129 Tb.2-15,p132-134, p138,p152 Tb.2-22|||See also . 0-1 km thick. Central marker of Salgash Subgroup. Formerly part of Empress Formation (of Fitton et al., 1975) and of Miralga Formation (Ingram, 1977). In West Pilbara metamorphosed chert and tuff (to 100m thick); in east metamorphosed dacitic lava,tuff etc.||Salgash Subgroup||Equivalent to Kelly Formation (at Copper Hills). Overlies Apex Basalt.|Metamorphosed dacitic lava, tuff and agglomerate, and chert; local sandstone, conglomerate and ultramafic rocks.|
14834|Panorama Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Felsic volcanic rocks: mainly rhyolite, quartz-feldspar porphyry, and felsic tuff.||||||07-NOV-08
14834|Panorama Formation|50189|4|Described|p9-10|Archean|Archean|Of the Salgash Subgroup. Interfingers with upper part of Apex Basalt. Ages: 3454 +/- 1Ma (Thorpe et al, 1992a), 3470 +/- 2Ma and 3458 +/- 2Ma (Thorpe, 1991, witten comm).||||||07-NOV-08
14834|Panorama Formation|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Underlies Euro Basalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Salgash Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|50423|6|Mentioned|p215 Fig.1||Archean|||||||07-NOV-08
14834|Panorama Formation|50427|5|Briefly described|p185 Fig.7|Archean|Archean|Age: 3432 Ma. Of Warrawoona Group.||||||07-NOV-08
14834|Panorama Formation|50430|4|Described|p160||Archean|Includes felsic volcanic and volcanogenic sedimentary rocks. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
14834|Panorama Formation|50544|5|Briefly described|p23, p19 Tb. 2 (amended)|Archean|Archean|Of the Warrawoona Group.  Flow-banded, fine-grained and porphyritic rhyoltie, banded chert, black chert.  Age: 3458+/-2, 3454+/-1 and 3445+/-2Ma.  max. thickness: <800m.  See also p21 Tb. 4.||||||07-NOV-08
14834|Panorama Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Felsic volcanic rocks, mainly rhyolite, quartz-feldspar porphyry and felsic tuff.  Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|60112|5|Briefly described|p108-111, p116. ||||3458+/-2 Ma (Thorpe et al, 1992).|Unit in Warrawoona Group.||Co-volcanic with the North Pole Monzogranite. Overlain by the Strelley Pool Chert.|1.3km thick felsic volcanic and volcaniclastic rocks.|
14834|Panorama Formation|60429|4|Described|p7, p9|Archean|Archean|Of the Salgash Subgroup. Overlain by Euro Basalt. Age: 3454+/-1Ma (U-Pb, Thorpe et al 1992a) and 3458+/-2Ma. Discontinuous felsic volcanic and chert unit.||||||07-FEB-11
14834|Panorama Formation|60636|5|Briefly described|p44, p52-53|Archean|Archean|Of the Warrawoona Group. Also referred to as the Kittys Gap volcano-sedimentary complex occurring between the Apex Formation below and Euro Formation above. Age: ~3446Ma. See also p35-36 Fig. 3.2, p37.||||||07-FEB-11
14834|Panorama Formation|61111|4|Described|p94, 98, p97 Fig. 3, p100,p102, p105||Paleoarchean|Topmost Formation of the Warrawoona Group. Deposited during emplacement of North Pole Monzogranite. Detailed description of lithology and geochemical analyses.|3459-3426 Ma|Warrawoona Group||Overlain by Euro Basalt. Unconformably overlain by the Strelley Pool Chert.|Dominantly volcaniclastic, but includes massive lavas, sub-volcanic intrusions and BIFs. Felsic volcanics|
14834|Panorama Formation|61253|5|Briefly described|p58, p52 Fig. 2|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Includes rhyolite. Geological Province: eastern Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Felsic volcaniclastic suite. Geological Province: North Pole Dome of the Pilbara Craton. See also p355 Tb. 1.||||||07-NOV-08
14834|Panorama Formation|61264|5|Briefly described|p64 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Mosquito Creek Basin/Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|61266|4|Described|p56, p58 Tb.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Overlain by Strelley Pool Chert. Age: 3458 Ma (McNaughton et al., 1993). Felsic lavas, tuffs and tuffaceous sandstone. Geological Province: Pilbara Craton.||||||07-NOV-08
14834|Panorama Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group. Age: 3458Ma.||||||07-NOV-08
14834|Panorama Formation|62427|5|Briefly described|p3-4, p6 Fig.3, p6, p11-12, p15-18  |Paleoarchean|Paleoarchean|Coppin Gap Greenstone Belt. REE and La/Yb contents detailed.|3446 +/- 5 Ma (U-Pb).|Of the Warrawoona Group.|Includes Kittys Gap Chert.|Overlies Apex Formation; is overlain by Euro Formation.|Interbedded agglomerates, flow-banded porphyries, volcaniclastics, rhyolites and rhyodacites; also silicified sediment and silicified rhyolite.|
14834|Panorama Formation|62979|5|Briefly described|p212 Fig. 1, p213|Archean|Archean|Of the Warrawoona Group. Felsic volcanics up to 1km thick. Age: 3.458-3.426Ga. Contains cross-bedded arenites. Geological Province: Pilbara Craton.||||||07-FEB-11
14834|Panorama Formation|63142|5|Briefly described|p487 Fig. 2|||Geological Province: Warrawoona Syncline. Felsic rocks.||||||29-MAR-07
14834|Panorama Formation|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Felsic volcanics.||||||07-NOV-08
14834|Panorama Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Age: 3433-3427Ma. Geological Province: Pilbara Craton. Felsic volcanic rock; local sedimentary rock; metamorphosed.||||||07-NOV-08
14834|Panorama Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Geological Province: Pilbara Craton. Rhyolitic, tuffaceous, volcaniclastic sandstone, including ash beds; well bedded; metamorphosed.||||||07-NOV-08
14834|Panorama Formation|63441|5|Briefly described|p4 Tb. 1, p20|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Overlies Apex Basalt, and Duffer Formation where basalt is missing. Unconformably overlain by Strelley Pool Chert (Kelly Group). Geological province: Pilbara Craton.||||||07-FEB-11
14834|Panorama Formation|63538|4|Described|p3 Fig. 2, p5, p8 Tb. 1, p9, p18|Archaean|Archaean|Of Salgash Subgroup (Warrawoona Group). Underlain by Apex Basalt.  Age: 3458-3426Ma. Geological Province: Pilbara Craton. Andesitic to rhyolitic volcanism. See p9 for more information.||||||17-APR-13
14834|Panorama Formation|63649|5|Briefly described|p201|Archean|Archean|Contains the "Kittys Gap Chert". Overlain by Strelley Pool Chert. Felsic volcanic rocks. Age: 3.359 - 3.426Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
14834|Panorama Formation|63854|5|Briefly described|p229 Fig.2, |||||Of the Warrawoona Group.||||
14834|Panorama Formation|64328|5|Briefly described|p54-55|Archean|Archean|Of Salgash Subgroup. Previously interpreted to be Duffer Formation - but volcanic breccia samples dating produced ages ranging between 3433-3427Ma, dates consistent with Panorama Formation. Volcaniclastic rocks with subordinate felsic lavas and chert.||||||07-FEB-11
14834|Panorama Formation|64405|5|Briefly described|p6, p13-14, p18|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Overlain by Strelley Pool Formation. Age: 3457+/-3Ma. Geological province: East Pilbara Terrane. Dominated by felsic volcanic rocks; includes brecciated rhyolite. See also p4 Fig. 3.||||||07-FEB-11
14834|Panorama Formation|64580|4|Described|map legend||Paleoarchean|Felsic volcanic and sedimentary rocks overlain by STRELLEY POOL CHERT; metamorphosed.||||||09-DEC-08
14834|Panorama Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group, Pilbara Supergroup). Felsic volcanic rock, local sedimentary rock; metamorphosed.||||||07-NOV-08
14834|Panorama Formation|64628|5|Briefly described|p170, p171 Fig.1, p172.  |Early Archean|Early Archean|Lateral equivalent of the volcano-sedimentary complex hosting the Kittys Gap chert. Fan-delta and shoreface deposits.||Unit in Warrawoona Group.|Includes Kittys Gap chert.||Volcanic tuff, graded beds and felsic lava flows.|
14834|Panorama Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Salgash Subgroup. Geological Province: Pilbara Craton. Generally, felsic tugg and andesitic basalt; weakly metamorphosed, dolerite, chert; metamorphosed.||||||07-FEB-11
14834|Panorama Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Salgash Subgroup. Age: 3458-3427Ma. Geological Province: Pilbara Craton. Quartz-sericite schist, derived from felsic volcanic rocks and quartz-rich sandstone; metamorphosed.||||||26-NOV-08
14834|Panorama Formation|64747|5|Briefly described|p94 fig 1, p95, p120|Paleoarchean|Paleoarchean|Eruptions were coeval with emplacement of North Pole Monzogranite as a subvolcanic laccolith.|c.3459-3434 Ma (U-Pb zircon: Thorpe et al., 1992)|Unit in Warrawoona Group.||||
14834|Panorama Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Salgash Subgroup. Over Apex Basalt. Age: 3458-3426 Ma (geochron: DR Nelson 2002 2001 2000; RI Thorpe et al 1992; ME Barley et al 1998; more). Rhyolite, schist, chert, volcaniclastics. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
14834|Panorama Formation|65008|4|Described|p5, p7-9, p20, p21, p27-29, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Geochronology by: Nelson (2001), Barley and McNaughton (1998), and Nelson (2000). Includes 5 separately mapped facies.|3433-3426 Ma|Of the Salgash Subgroup||Overlain by the Strelley Pool Chert.|Felsic agglomerate and minor felsic tuff and andesitic basalt, locally silicified; felsic tuff and minor felsic agglomerate and andesitic basalt, locally silicified; layered grey-blue and white chert; minor massive cream chert. Weakly metamorphosed.|
14834|Panorama Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as three sub-units.|c.3458 - 3427 Ma (Nelson 2000).|Of Salgash Subgroup.||Is overlain by Strelley Pool Chert.|Metamorphosed felsic volcanic and sedimentary rocks; weakly metamorphosed, locally silicified, felsic, tuff and aggregate.|
14834|Panorama Formation|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as three sub-units.|c.3433 - 3427 Ma (Barley et al. 1998).|Of Salgash Subgroup.|||Felsic volcanic and local sedimentary rocks; felsic volcaniclastic rocks including debris-flow deposits, autobreccia and agglomerate, minor chert, local basaltic andesite; felsic tuffaceous  rocks, agglomerate and volcanic breccia. All metamorphosed|
14834|Panorama Formation|65827|3|Fully described|p6 Tb.1, p12-13 Tb.3-4, p15, p19-21|Paleoarchean|Paleoarchean|Of Warrawoona Group. Intruded by Carbana and Mondana Monzogranites, Dalton Suite; overlies Apex Basalt, Fig Tree Gneiss; separated from Apex Basalt by a Shear Zone; underlies Strelley Pool Chert, disconformably underlies Euro Basalt. Metamorphosed sparsely porphyritic rhyolite and dacite, quartz-sericite schist after felsic volcanic rock, felsic agglomerate. 3433 +/- 2 Ma (SHRIMP U-Pb zircon; Nelson 2000).||||||
14834|Panorama Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Salgash Subgroup. Age shown as 3449-3427 Ma. Felsic volcanic rock; local sedimentary rock; metamorphosed.||||||09-APR-13
14834|Panorama Formation|66122|5|Briefly described|p75, 85|Archean|Archean|Mount Goldsworthy greenstone belt, NE Pilbara Craton.||Warrawoona Group.|||Felsic volcanic rocks and sedimentary rocks; includes jasper and siderite.|
14834|Panorama Formation|66217|4|Described|p1, p8, p14, p15, p27, p60.|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. Hosts Pb-Zn mineralisation at Quartz Circle in the McPhee Dome. Up to 2000 m thick.|3458-3426 Ma (U-Pb zircon: Thorpe et al. 1992).|Upper unit in Salgash Subgroup.||Conformably overlies Apex Basalt. Unconformably overlies Duffer Formation.|Rhyolitic and dacitic volcaniclastic rocks; massive rhyolite and dacite.|
14834|Panorama Formation|66664|6|Mentioned|p8.|||||Unit in Warrawoona Group.|||Felsic volcaniclastic rocks. Local dacitic volcaniclastic breccia and sandstone.|
14834|Panorama Formation|66745|4|Described|pp53-56.|Paleoarchean|Paleoarchean|Local uplift; erosion of Apex Basalt.|3449-3427 Ma.|Unit in Salgash Subgroup.||Overlies Apex Basalt. Overlies Duffer Formation in western Warralong, Panorama and Coongan greenstone belts. Unconformably overlain by Strelley Pool Formation.|Felsic volcanic rocks; minor jaspilite, siliciclastic rocks.|
14834|Panorama Formation|67130|6|Mentioned|p13, p17, p63, p85|Paleoarchean|Paleoarchean||3434 +/- 5 Ma (SHRIMP U/Pb)|Warrawoona Group||Overlies Antarctic Creek Member, disconformably overlain by Strelley Pool Formation|Dacite.|
14834|Panorama Formation|67197|5|Briefly described|p2, p4, p6|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3450-3427 Ma.|Salgash Subgroup.||Is overlain ?conformably by Strelley Pool Formation.||
14834|Panorama Formation|67201|5|Briefly described|p7 Fig.4, p8, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane. Detrital zircons: 3724 Ma (Thorpe et al., 1992).|c. 3430 Ma|Salgash Subgroup||||
14834|Panorama Formation|67269|5|Briefly described|p5, p6 Fig.3, p8-9, p12-13, p26|Paleoarchean|Paleoarchean|The unconformity with the Duffer Formation indicates erosion of 11-12 km of Warrawoona Group rocks in the East Pilbara Terrane. Other ages include 3447 +/- 12 Ma (maximum depositional age: SHRIMP zircon U-Pb, Van Kranendonk 2010) and 3434 +/- 5 Ma (Nelson, 2000).|3449-3427 Ma.|Warrawoona Group.||Overlies Duffer Formation, and locally the Mount Ada Basalt unconformably. Is overlain unconformably by Strelley Pool Formation.|Felsic volcanic rocks, sandstone and chert.|
14834|Panorama Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3449-3427 Ma.|Salgash Subgroup.||||
14834|Panorama Formation|67668|5|Briefly described|Fig. 2-4; p. 154, 156, 161; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton. Possible evidence of early life is reviewed.|3458 - 3427 Ma.|Warrawoona Group||Unconformably underlies the Strelley Pool Formation, overlies the Apex Basalt.|Contains a diverse range of lithologies, dominated by felsic volcaniclastics (now silicified), with lesser amounts of mafic and felsic lavas, and minor hydrothermal chert.|
14834|Panorama Formation|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane.|3449 - 3427 Ma|Of Salgash Subgroup.||Overlies Apex Basalt. Unconformably overlies Duffer Formation. Unconformably overlain by Strelley Pool Formation.|Felsic volcanics, minor jaspilite, siliciclastic rocks|
14834|Panorama Formation|68280|5|Briefly described|p2, p4, p19, p22 fig 19|||||||Overlies Apex Basalt, disconformably overlain by Strelley Pool Formation|Siliciclastic rocks, jaspilite and felsic volcanic rocks.|
14834|Panorama Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|Detailed lithology discussed in map legend; the 3 facies are mapped separately.|3449-3427 Ma (Thorpe et al. 1992).|Of the Salgash Subgroup.|||Felsic volcaniclastic rock, minor chert, local basaltic andesite; felsic tuffaceous volcaniclastic rock, minor agglomerate and volcanic breccia; felsic volcaniclastic conglomerate and sandstone, minor felsic schist, carbonate cemented; metamorphosed.|
14834|Panorama Formation|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Ages from Thorpe et al. (2002) and De Vries (2004). The 4 facies are mapped separately.|3449-3427 Ma|Of the Salgash Subgroup|||Metafelsic volcanic rock, schistose; felsic volcaniclastic conglomerate and sandstone, minor felsic schist; porphyritic to aphanitic felsic dyke; felsic volcaniclastic rock with debris-flow deposits, agglomerate, minor chert, local basaltic andesite.|
14834|Panorama Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Ages from Thorpe et al. (1992), Barley et al. (1998) and de Vries (2004).|c.3458-3427 Ma|Of the Salgash Subgroup.|||Rhyolitic, tuffaceous, volcaniclastic sandstone, including ash beds; well bedded; metamorphosed.|
14834|Panorama Formation|68284|5|Briefly described|p4-7|Paleoarchean|Paleoarchean|Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|3449-3427 Ma (Van Kranendonk et al., 2007).|Salgash Subgroup (topmost Warrawoona Group).||Overlies Apex Basalt. Is overlain paraconformably to disconformably by Strelley Pool Formation.|Flow-banded, fine-grained and porphyritic rhyolite, fragmental volcanic rocks, and minor banded and black chert.|
14834|Panorama Formation|68312|5|Briefly described|p102-104, 114|Archean|Archean|North Pole Dome, Pilbara Craton.|~3.7-3.3 Ga.|Warrawoona Group.|||Felsic volcanic and volcaniclastic rocks, rhyolitic to dacitic composition; minor tuff, volcanic sandstone and bedded cherts.|
14834|Panorama Formation|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. The six facies are mapped separately.|3449-3427 Ma (Thorpe et al. 1992; De Vries, 2004)|Of the Salgash Subgroup.|||Quartz-porphyritic rhyolite; felsic tuffaceous and volcaniclastic rocks; volcaniclastic conglomerate and sandstone; quartz-rich sandstone; chert: all metamorphosed.|28-APR-14
14834|Panorama Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as 11 separate unnamed units. Geochronology by Thorpe et al. (2002) and De Vries (2004). See map legend for a detailed lithological description. Includes a porphyritic to aphanitic felsic dyke.|3449-3427 Ma|Of the Salgash Subgroup. |||Metafelsic volcanic rock; chert; banded iron-formation; felsic volcaniclastic conglomerate and sandstone; felsic volcanic breccia; felsic, tuffaceous volcaniclastic rocks; rhyolitic tuffaceous volcaniclastic sandstone.|02-MAY-14
14834|Panorama Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Banded iron formation; sometimes jaspilitic. Felsic volcaniclastic conglomerate, sandstone and breccia. Tuffaceous felsic volcaniclastic rocks. Age derived from samples of felsic volcanic rock and volcaniclastic metasandstone (age is of protolith deposition)  (142952.1.pdf, 160958.1.pdf)|3434 Ma +/- 5 Ma  3453 +/- 6 Ma (SHRIMP)|Salgash Subgroup|||Felsic volcanic rock; local sedimentary rock; metamorphosed. Metafelsic volcanic rock, ultramafic schist, porphyritic rhyolite and porphyritic micromonzogranite. Quartz rich sandstone, siltstone, shale, layered chert.|
14834|Panorama 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 Salgash Subgroup.||Overlain by Strelley Pool Chert.|Felsic volcanic and sedimentary rocks; metamorphosed.|
14834|Panorama 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. Panorama Formation and Tambina Supersuite.|3449-3427 Ma; 3430 Ma|Salgash Subgroup||Unconformity at top.|Felsic volcanic rocks; with jaspilite, siliciclastic rocks.|
14834|Panorama Formation|69566|6|Mentioned|p236|||East Pilbara Granite-Greenstone Terrane.||Warrawoona Group.||Overlies Apex Basalt. Is overlain by Euro Basalt (Kelly Group).||
14834|Panorama Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Warrawoona Group.||||
14834|Panorama 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. Outcrops on all sides of the North Pole Dome over a strike length of 100 km. Sample GSWA 142952 (porphyritic felsic tuff) yielded an interpreted igneous crystallisation age of 3434+\-5 Ma (weighted mean 207Pb/206Pb). Sample GSWA 142972 (qtz-rich metasedimentary rock0 yielded an interpreted igneous crystallisation age of 3433+\-6 Ma for the volcanigenic component within the metasedimentary rock (weighted mean 207Pb/206Pb). Sample GSWA 160221 (tuffaceous rhyolite) yielded an interpreted igneous crystallisation age of 3430+\-4 Ma for the rhyolite (weighted mean 207Pb/206Pb). Sample GSWA 160958 (volcaniclastic sandstone) yielded an interpreted maximum depositional age of 3443+\-4 Ma for the sedimentary protolith (weighted mean 207Pb/206Pb). Sample GSWA 168989 (volcaniclastic metasandstone) yielded an interpreted igneous crystallisation age of 3491+\-4 Ma for the volcanigenic component of the metasandstone (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.|3449-3427 Ma (inferred)|Unit of Salgash Subgroup.||Overlain unconformably by Strelley pool Formation.|Banded iron-formation, felsic volcanic breccia, felsic volcanic and volcaniclastic conglomerate, sandstone and tuffs; chert, quartz-porphyritic rhyolite, quartz sandstone, shale siltstone, micromonzogranite dykes and intrusions.|
14834|Panorama Formation|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.46-3.43 Ga.|Warrawoona Group.||Overlies Apex Basalt.||
14834|Panorama Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Salgash Subgroup.||||
14834|Panorama Formation|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.||Unit of Pilbara Supergroup.|||Interbedded black organich-matter rich layered cherts (interbedded stratigraphically and as hydrothermal veins i.e. silica dikes), thick coarsely crystalline barite, conglomerate, sand-stone and carbonates, and pillow and komatiitic basalts.|
14834|Panorama Formation|70729|5|Briefly described|p163|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.45 Ga|||Underlain by Apex Basalt.|Felsic volcanics.|
14834|Panorama Formation|70733|6|Mentioned|p103-104, 106|||Pilbara Craton.|3446 +/- 5 Ma (de Vries et al., 2006).|||Overlies Apex Basalt. Is overlain by Fortescue Group.|Felsic volcanics.|
14834|Panorama Formation|70775|5|Briefly described|p12|Paleoarchean|Paleoarchean|East Pilbara.|c. 3430 Ma|Warrawoona Group||Overlies the Apex Basalt. Unconformably overlain by the Strelley Pool Formation.||
14834|Panorama Formation|70834|5|Briefly described|p298, 312|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.|3446 Ma.||Kittys Gap chert.|Overlies Apex Basalt. Is overlain unconformably by Strelley Pool Formation.|BIF.|
14834|Panorama Formation|70884|5|Briefly described|p123-124|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3.45-3.43 Ga|Unit of Salgash Subgroup.||Overlain unconformably by Strelley Pool Formation. Underlain by Apex Basalt.||
14834|Panorama Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|Max age 3448+/-6 Ma, min 3424+/-16 Ma.|Salgash Subgroup|||Felsic volcanic rock; local sedimentary rock; metamorphosed.|
14834|Panorama Formation|72064|5|Briefly described|p66,76|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. U-Pb zircon ages include 3430+\-4 Ma (Nelson, 2002) and 3427 +\-2 Ma (Nelson, 2001) in the Coongan and Kelly greenstone belts, respectively.||Unit of Warrawoona Group.||Uppermost unit of Warrawonna Group. Overlain unconformably by Strelley Pool Formation. Underlain by Apex Basalt, or unconformably by Duffer Formation.||
14834|Panorama Formation|72251|5|Briefly described|p51,53-55,64|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Rhyolitic unit contemporaneous with Tambina Supersuite (Van Kranendonk et al., 2006). Contains 3.724 Ga xenocrystic zircon (Thorpe et al., 1992), could indicate existence of even older crust within the EPT.||Unit of Salgah Subgroup.||Overlain unconformably by Strelley Pool Formation. Underlain by Apex Basalt.|Rhyolitic volcanic rocks.|11-FEB-20
14834|Panorama Formation|72668|5|Briefly described|p3-10, p17-19, p24, p26, p27|||East Pilbara Terrane. Deposited in shallow water conditions. Volcanics contemporaneous with Tambina Supersuite.|c. 3460 - 3430 Ma|Salgash Subgroup?, top of Warrawoona Group||Overlies the Apex Basalt. Unconformably overlain by Kelly Group.|Andesitic to rhyolitic volcanics with some dacite dominated deposits.|13-JAN-22
14834|Panorama Formation|73160|6|Mentioned|p2 Fig.1, p3|||Pilbara Craton. Top of the Warrawoona Group.||Warrawoona Group|||Felsic volcanic rocks.|
14834|Panorama Formation|73598|5|Briefly described|p1208-1212|Paleoarchean|Paleoarchean|East Pilbara Terrane. Type locality is at the S margin of the North Pole dome.|3450-3430 Ma.|Salgash Subgroup.||Overlies Apex Basalt. Is overlain unconformably by Strelley Pool Formation.|Felsic volcanic rocks, including rhyolite.|
14839|Panton Formation|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Includes the Shady Camp and Corby Limestone Members.  Geological Province: Ord Basin.||||||
14839|Panton Formation|23821|5|Briefly described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.||||||
14839|Panton Formation|24303|6|Mentioned|p63 Appendix|||Geological Province: Ord Basin. Correlative Of Gum Ridge Formation.||||||
14839|Panton Formation|28255|3|Fully described|p98|Middle Cambrian|Middle Cambrian|Of the Negri Group. Consists of a lower siltstone, middle fossiliferous limestone and an upper limestone; minor shale and gypsum. Conformably overlies Linnekar Limestone; conformably underlies Hudson Fm. Max. thickness: 190m. See also Table 9 (before p83)||||||
14839|Panton Formation|32172|4|Described|Table 2|||Middle Camb.||||||
14839|Panton Formation|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Purple and green siltstone, minor shale, gypsum bands, fossiliferous limestone.  Conformably overlain by the Hudson Formation; conformably overlies the Linnekar Limestone.||||||17-NOV-04
14839|Panton Formation|32648|6|Mentioned|p32|||M.Camb.||||||
14839|Panton Formation|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
14839|Panton Formation|36551|6|Mentioned|Table 16|||||||||
14839|Panton Formation|36890|3|Fully described|p397|||Formerly Panton Shale.||||||14-NOV-06
14839|Panton Formation|40993|6|Mentioned|Fig.1|||||||||
14839|Panton Formation|40996|6|Mentioned|p405|||||||||
14839|Panton Formation|41840|1|Redefined|p42|Middle Cambrian||Incorporates the former Panton Shale, Shady Camp Limestone, Negri River Shale, Corby Limestone, Hudson Sh.||||||14-NOV-06
14839|Panton Formation|41864|4|Described|p19|||Includes units formerly known as Panton, Negri River, Hudson Shales, Corby Shady Camp Lsts.||||||
14839|Panton Formation|41865|5|Briefly described|Map legend|Middle Cambrian||||||||
14839|Panton Formation|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
14839|Panton Formation|42070|6|Mentioned|p4|||||||||
14839|Panton Formation|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
14839|Panton Formation|44317|4|Described|Table 4||Cambrian|||||||
14839|Panton Formation|44318|14|Not recorded|map legend||Middle Cambrian|Mid.Cambrian||||||
14839|Panton Formation|44363|5|Briefly described|p.6,18,21||Middle Cambrian|Middle Cambrian.||||||
14839|Panton Formation|44364|14|Not recorded|map legend|||||||||
14839|Panton Formation|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
14839|Panton Formation|45047|6|Mentioned|p126|||See also p128.||||||14-NOV-06
14839|Panton Formation|48943|3|Fully described|p110|||||||||
14839|Panton Formation|60419|3|Fully described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Linnekar Limestone. Conformably overlain by Eagle Hawk Sandstone. Max. thickness: 308 m. Maroon gypsiferous siltstone and shale, with two limestone members. Peritidal. Geological Province: Ord Basin.||||||
14839|Panton Formation|60519|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Siltstone and mudstone; minor feldspathic sandstone, and limestone. Geological Province: Ord Basin.||||||03-NOV-04
14839|Panton Formation|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Includes two members: Corby Limestone and Shady Camp Limestone Members.  Conformably overlies the Linnekar Limestone; conformably overlain by Eagle Hawk Sandstone.  Geological Province: Ord Basin.||||||24-NOV-04
14839|Panton Formation|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.|||Includes Shady Camp and Corby Limestone Members.|||28-MAR-12
14839|Panton Formation|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
14839|Panton Formation|67352|6|Mentioned|p21|Middle Cambrian|Middle Cambrian|Ord Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
14839|Panton Formation|67860|4|Described|p417 fig 4-85, p419 Tb. 4-18, p421|Middle Cambrian|Middle Cambrian|105-308 m thick. Type section details given. Fossiliferous. Said to include "Hudson Formation" of Dow et al. (1964) [??].||Negri Subgroup|Includes Corby and Shady Camp, Limestone Members.|Conformably overlies Linnekar Limestone. Is overlain conformably by Eagle Hawk Sandstone.|Purple siltstone with sandstone and mudstone; minor limestone.|
14839|Panton Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3||Ord Basin||Negri Subgroup|||Purple siltstone; interbedded sandstone and mudstone; minor limestone.|04-AUG-15
14839|Panton Formation|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv.||Negri Subgroup|||Purple siltstone; interbedded sandstone and mudstone; minor limestone.|
14839|Panton Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Overlies Linnekar Limestone. Is overlain by Eagle Hawk Sandstone.||12-JUL-16
14839|Panton Formation|69446|6|Mentioned|p31:3|||Ord Basin. Strong species-level similarity with correlative faunas of Tindall Limestone (Daly Basin).||||||12-JUL-16
14839|Panton Formation|69447|6|Mentioned|p32:2|||Ord Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
14839|Panton Formation|69448|4|Described|p33:2-6, 8|Middle Cambrian|Middle Cambrian|Redefined by Mory and Beere (1985) to include five superseded Formation-rank units of Traves (1955). The upper part was formerly the Hudson Formation. Ord Basin. 308m thick. Peritidal deposits; restricted shallow subtidal between named Members. Widely distributed but poorly exposed. Typically forms sandy vertosol ("black soil") plains. Unfossiliferous except for the medial interval bracketed by named Members, which contains trilobites (including Redlichia and Xystridura), brachiopods, hyoliths, molluscs, disarticulated echinoderms, chancelloriids and sponge spicules. Hosts a number of uneconomic base metal anomalies.||Negri Subgroup.|Shady Camp, Corby, Limestone Members.|Conformably and gradationally overlies Linnekar Limestone. Is overlain conformably by Eagle Hawk Sandstone.|Maroon gypsiferous siltstone, mudstone, minor feldspathic sandstone and limestone; limestone, marl and thin sandstone beds between named Members.|12-JUL-16
14839|Panton Formation|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Purple siltstone; interbedded sandstone and mudstone; minor limestone|
14839|Panton Formation|69673|5|Briefly described|p142, p192, p193|Cambrian|Cambrian|308m thick.||Negri Subgroup|Includes Shady Camp Limestone Member, Corby Limestone Member|Overlies Linnekar Limestone, overlain by Eagle Hawk Sandstone|Gypsiferous siltstone and mudstone, fossiliferous limestone and marl and minor thin sandstone beds.|
14839|Panton Formation|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Siltstone; interbedded sandstone, mudstone and minor limestone.|
14839|Panton Formation|70752|6|Mentioned|p131|||Ord Basin. Contains a fragment of brachiopod Westonia-like ornamentation of limited comparative value.||||||
14839|Panton Formation|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|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.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Purple siltstone; interbedded sandstone and mudstone; micritic and oncolitic limestone|
14839|Panton Formation|71800|4|Described|p25-p27|Middle Cambrian|Middle Cambrian|Ord Basin. Hosts age diagnostic fossils such as the brachiopod Billingsella and Wimanella, girvanellids and stromatolites.||Negri Subgroup|Includes the Shady Camp Limestone Member and the Corby Limestone Member.|Overlies the Linnekar Limestone. Conformably (gradationally) overlain by the Eagle Hawk Sandstone.|Purple siltstone, flaggy sandstone and limestone.|
14839|Panton Formation|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Linnekar Limestone, underlies the Eagle Hawk Sandstone.||
14869|Pargee Sandstone|22446|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|23809|4|Described|p9, p4|Paleoproterozoic|Paleoproterozoic|Interbedded conglomerate, quartz arenite and minor siltstone. Overlain by Gardiner Sandstone; unconformably overlies Killi Killi Formation.  Age: 1835Ma (inferred by Blake et al, 1999); <1845-1840Ma (Cooper and Ding, 1997).||||||07-NOV-08
14869|Pargee Sandstone|29809|6|Mentioned|Table 1|||||||||
14869|Pargee Sandstone|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|29812|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14869|Pargee Sandstone|29813|4|Described|Table 2|||||||||
14869|Pargee Sandstone|29818|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|31361|4|Described|Table 2|||||||||
14869|Pargee Sandstone|31362|4|Described|Table 1|||||||||
14869|Pargee Sandstone|33102|6|Mentioned|Fig.2|||||||||
14869|Pargee Sandstone|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|36902|6|Mentioned|p12|||||||||
14869|Pargee Sandstone|37462|6|Mentioned|p279|||||||||
14869|Pargee Sandstone|39887|6|Mentioned|p452|||||||||
14869|Pargee Sandstone|41125|6|Mentioned|p30|||||||||
14869|Pargee Sandstone|41883|5|Briefly described|p65|||||||||
14869|Pargee Sandstone|42643|6|Mentioned|p5|||||||||
14869|Pargee Sandstone|43631|6|Mentioned|p10|||||||||
14869|Pargee Sandstone|45112|6|Mentioned|p17|||||||||
14869|Pargee Sandstone|45140|2|Defined|p12-15, 17-18, p20, p22, p39, p41, p43|Paleoproterozoic|Paleoproterozoic|See also p54, p73, Appx.p8. Blake et al. (1975). The Granites-Tanami Block. Named after Pargee Range. The type section runs for 800m along a gully between 19deg 38'20"S, 129deg 12'30"E and 19deg 38'30"S, 129deg 12'15"E, Tanami sheet area. 1500m thick. Crops out as strike ridges up to 30m high, most extensively W and S of Pargee Range. Mainly steeply-dipping to overturned and tightly folded.|c.1800 Ma.|||Unconformably overlies Killi Killi and Mount Charles Beds (Tanami Complex). Is overlain unconformably by Gardiner and Muriel Range Sandstones.|Interbedded sublithic, lithic, and quartz arenite, conglomerate and greywacke. Arenites are mainly poorly sorted and medium-coarse grained; beds about 1m thick with common cross-bedding and ripple marks.|
14869|Pargee Sandstone|45167|5|Briefly described|Fig.27|||||||||
14869|Pargee Sandstone|46830|6|Mentioned|p29|||||||||
14869|Pargee Sandstone|46864|5|Briefly described|p37|||||||||
14869|Pargee Sandstone|48950|2|Defined|p22|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone; sublithic and lithic arenite, quartz arenite; cream, pink, purple; sandstone poorly sorted, medium- to coarse-grained; conglomerate contains jasper clasts.||||||07-NOV-08
14869|Pargee Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone; sublithic and lithic arenite, quartz arenite.||||||07-NOV-08
14869|Pargee Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14869|Pargee Sandstone|50589|6|Mentioned|p2.1|||||||||
14869|Pargee Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Conglomerate, sandstone and siltstone: sublithic and lithic arenite, quartz arenite.||||||07-NOV-08
14869|Pargee Sandstone|61056|5|Briefly described|p777|||Overlies the Tanami Group.||||||
14869|Pargee Sandstone|61861|3|Fully described|p15-17, 3, 4,10,12,23, Figs.23-28, Map 1|Orosirian|Orosirian|Deposited in small extensional basins on top of deformed MacFarlane Peak and Tanami Groups. Non- to weakly magnetic. Deposition post-dates folding of Tanami Group, hence age is less than 1840 Ma. Tentatively correlated with Moola Bulla Formation.|1835 Ma inferred from correlation|||Unconformably overlies Dead Bullock Formation, Killi Killi Formation. Unconformably overlain by the Gardiner Sandstone, Birrindudu Group.|Dominated by interbedded thick-bedded quartz and lithic arenites and conglomerate. Pebbly sandstone and conglomerate are prominent at base. Most clasts are subrounded vein quartz, greywacke, siltstone and jasper derived from Killi Killi Formation.|
14869|Pargee Sandstone|62377|4|Described|p5, 7|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Tanami Group. Quartz sandstone, lithic arenite and conglomerate. Unconformably overlain by Birrindudu Group. Overlies Killi Killi Formation and Dead Bullock Formation. Age : 1734 +/- 25Ma.||||||07-NOV-08
14869|Pargee Sandstone|62580|6|Mentioned|p10, p21|||Shallow marine sediments.||||||07-FEB-11
14869|Pargee Sandstone|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Sandstone, conglomerate, siltstone: sublithic and lithic arenite, quartz arenite, jasperlitic conglomerate.||||||07-NOV-08
14869|Pargee Sandstone|63261|3|Fully described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Gardiner Sst (Birrindudu Gp); unconformable on Killi Killi Sst. Max dep age: 1768+/-14Ma. Thick succession of interbedded conglomerate, pebbly sandstone, quartz arenite + minor siltstone - more lith.detail included.||||||07-FEB-11
14869|Pargee Sandstone|63866|6|Mentioned|p99|||||||||
14869|Pargee Sandstone|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: <1760Ma. Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone. Conglomerate, cross-bedded sandstone and quartz sandstone and shale; minor dolomitic sandstone.||||||
14869|Pargee Sandstone|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone; minor conglomerate.||||||09-DEC-08
14869|Pargee Sandstone|64662|5|Briefly described|p28, p30 Fig. 3, p40, 44|Statherian|Statherian|Age: ~1.77 - 1.64 Ga, based on combo of youngest detrital zircons dates, diagenetic xenotime growth, age of Limbunya Group rocks (which overlie Birrindudu Group). Sandstone and conglomerate. Unconformably overlain by Gardiner Sandstone. Tanami region.||||||07-FEB-11
14869|Pargee Sandstone|64675|5|Briefly described|p9, p10, Fig.2, p16, Fig.24, p17, p24|Paleoproterozoic|Paleoproterozoic|Forms a prominent north-northeast orientated strike ridge east of the Pargee Fault. A high energy molasse deposit consistent with sedimentation in response to active deformation and uplift of underlying basement groups (Hendrickx et al 2000). See also Map 1.||||Unconformably underlain by the Tanami Complex. Unconformably underlain by the Killi Killi Formation.|Fines rapidly upward from thick bedded pebbly conglomerate (with vein quartz, chert and red jasper clasts) to quartz gritstone and medium to fine grained sandstone and siltstone.|19-MAR-14
14869|Pargee Sandstone|64722|5|Briefly described|Fig. 2 p3-6, p10|Statherian|Statherian|Maximum age from youngest detrital zircon (Cross and Crispe, 2007). Minimum age from Limbunya Group which lies stratigraphically above it. Interpreted as a platformal cover succession.|1768 +/- 14 Ma maximum.|||Unconformably overlain by Birrindudu Group.||11-APR-12
14869|Pargee Sandstone|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|<1735 Ma.|||||
14869|Pargee Sandstone|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Statherian||~1765-1630 Ma.|||Unconformably overlies Mount Charles Formation and unconformably overlain by Birrindudu Group.||20-APR-12
14869|Pargee Sandstone|64734|5|Briefly described|p186 Fig.1||Statherian|<1735 Ma||||||14-SEP-09
14869|Pargee Sandstone|64956|6|Mentioned|p7|||In Tanami region.||||||07-FEB-11
14869|Pargee Sandstone|65074|6|Mentioned|p349, p351 fig 4-37|Proterozoic|Proterozoic|Of North/Centre Birrindudu Basin. Early Proterozoic. 1500 m thick.||||Unconformably overlain by Gardiner Sandstone.|Arenites, pebbly conglomerates.|
14869|Pargee Sandstone|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||02-FEB-10
14869|Pargee Sandstone|65324|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65326|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||02-FEB-10
14869|Pargee Sandstone|65327|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65328|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65338|6|Mentioned|p21.|||Tanami Region. Previously, correlated with Reynolds Range Group (Blake et al. 1979).||||||
14869|Pargee Sandstone|65349|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65350|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65351|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||
14869|Pargee Sandstone|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Conglomerate, sandstone, siltstone; non to weakly magnetic||||||02-FEB-10
14869|Pargee Sandstone|65354|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65355|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65356|5|Briefly described|Map legend|Orosirian|Orosirian|Not shown on map||||||
14869|Pargee Sandstone|65358|5|Briefly described|p7|Statherian|Statherian|In Tanami Region. Quartz sandstone, lithic arenite and conglomerate. Represents syn-tectonic sedimentation during the 1730 Ma Strangways Orogeny.||||||
14869|Pargee Sandstone|66129|5|Briefly described|p213, p214 Fig.1, p216 Fig.3|Statherian|Statherian|1758-1700 Ma. Unconformably underlies Birrindudu Group, unconformably overlies Ware Group.||||||
14869|Pargee Sandstone|66468|5|Briefly described|p16-17 Figs.2-4, p19, p21 Fig.6, p22|Statherian|Statherian|<1735 Ma. 1760 Ma (detrital zircon) to 1632 +/-3 Ma (diagenetic xenotime). ~1300m thick. Underlies Birrindudu Group unconformably.||||||
14869|Pargee Sandstone|66860|6|Mentioned|p6 Tb.1|||Tanami Region. Coeval with deposition of Ledan and (?) Oonagalabi packages (Arunta Region), and Hanlon Subgroup and upper parts of Tomkinson Creek Group (Tennant Region).||||||
14869|Pargee Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlies Tanami Group units. Is unconformably overlain by Gardiner Sandstone and Muriel Range Sandstone.|Conglomerate, sandstone, siltstone.|
14869|Pargee Sandstone|67824|6|Mentioned|p385 Fig.2|Paleoproterozoic|Orosirian||< 1735 Ma|||||
14869|Pargee Sandstone|67826|6|Mentioned|p401 Fig.2, p403|Statherian|Statherian|Relatively flat-lying sedimentary rocks.|~ 1770-1640 Ma|||||
14869|Pargee Sandstone|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|<1735 Ma|||||
14869|Pargee Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.|||||Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone; conglomerate; cross-bedded sandstone; minor dolomitic sandstone.|
14869|Pargee Sandstone|68733|6|Mentioned|p186, p187 Fig.6|||Tanami region.||||Unconformably overlain by the Birrindudu Group. Unconformably underlain by the Mount Charles Formation.||05-DEC-17
14869|Pargee Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Sandstone; minor conglomerate.|04-AUG-15
14869|Pargee Sandstone|69253|5|Briefly described|p747 Fig.1, p748-749|Paleoproterozoic|Paleoproterozoic||< 1735 Ma.|||Unconformably overlies Tanami Group. Is overlain unconformably by Birrindudu Group.|Sandstone and conglomerate.|
14869|Pargee Sandstone|69383|6|Mentioned|p70|||Tanami Region. Detrital zircon spectra compared to Utopia Quartzite spectra.||||||
14869|Pargee Sandstone|69426|5|Briefly described|p11:3, 5, 7, 10, 14|||Crops out on W side of Coomarie Dome. SHRIMP U-Pb (detrital) zircon maximum depositional age.|<1768 +/- 14 Ma (Cross and Crispe, 2007).|||Unconformably overlies Killi Killi Formation. Is overlain unconformably by Gardiner Sandstone.|Interbedded shallow-marine to fluvial conglomerate, quartz sandstone and minor siltstone.|12-JUL-16
14869|Pargee Sandstone|69431|6|Mentioned|p16:1|||Tanami Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
14869|Pargee Sandstone|69432|5|Briefly described|p17:2|||Youngest detrital zircon maximum depositional age.|1768 +/- 14 Ma (Cross and Crispe, 2007).|||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
14869|Pargee Sandstone|69587|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: North Australian Craton. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1760-1735 Ma (inferred)||||Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone, cross-bedded sandstone, conglomerate, minor dolomitic sandstone, shale.|
14869|Pargee Sandstone|69618|6|Mentioned|p90|Paleoproterozoic|Paleoproterozoic||<1735 Ma.|||||
14869|Pargee Sandstone|69747|5|Briefly described|p263||Paleoproterozoic|Geological province: Tanami Block, North Australian Craton.|< 1735 Ma|||||
14869|Pargee Sandstone|69917|6|Mentioned|p87|||Tanami Region. One of a number of North Australian Craton sources of zircons older than 1900 Ma.||||||
14869|Pargee Sandstone|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|These three facies are mapped separately.|1760-1735 Ma.||||Conglomerate, cross-bedded sandstone and quartz sandstone, siltstone and shale; minor dolomitic sandstone. Siltstone and mudstone; minor fine-grained, micaceous quartz sandstone. Quartz sandstone.|
14869|Pargee Sandstone|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Conglomerate; cross-bedded sandstone and quartz sandstone, siltstone and shale; minor dolomitic sandstone.|
14869|Pargee Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1735-1760 Ma||||Sandstone; minor conglomerate|
14869|Pargee Sandstone|70291|4|Described|p178,180-181|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Maximum depositional age of ~1735 Ma (but also suggested to be 1758+\-15 Ma; cross and Crispe, 2006?). Also constrained by a 1632+\-3 Ma age of xenotime associated with epigenetic REE-Th-U mineralisation (Vallini et al. 2006). Coeval with Fiddler Lake Granite emplacement.|<1735 Ma|||Overlain unconformably by Birrindudu Group.|Interbedded conglomerate, quartz arenite and minor siltstone|
14869|Pargee Sandstone|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||||Sandstone, conglomerate, siltstone; sublithic and lithic sandstone, quartz sandstone, conglomerate with jasperlitic and volcanic clasts.|
14869|Pargee Sandstone|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|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 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1760-1735 Ma (inferred)||||Cross bedded, medium to coarse and locally pebbly sublithic sandstone with minor conglomerate|
14869|Pargee Sandstone|71348|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami Region, North Australian Craton. Maximum depositional age c. 1780 Ma Maidment et al., 2005; Cross and Crispe, 2007; Hollis et al., 2013; Kositcin et al., 2015).|< 1780 Ma.|||||
14869|Pargee Sandstone|71349|5|Briefly described|p724-725, p737|Paleoproterozoic|Paleoproterozoic|Tanami Region. Relatively flat-lying sedimentary rocks. Contains zircons aged c.3.1 Ga (significance explained).|1758-1700 Ma.|||||
14869|Pargee Sandstone|71397|6|Mentioned|p5|Statherian|Statherian|Geological province: Granites-Tanami Orogen.||||||
14869|Pargee Sandstone|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1768+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz arenite.|
14869|Pargee Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic||||||Sandstone; minor conglomerate.|
14869|Pargee Sandstone|73083|6|Mentioned|p24|||Intruded by granite of the Tanami Orogen.||||||
14869|Pargee Sandstone|73089|4|Described|p3, p6-10, p29-31|Statherian|Statherian|Restricted area west of Coomarie Dome. 1.5 km thick. High energy shallow marine to fluvial depositional setting. Broadly coarsens up sequence. Post-dates granitic magmatism.|< c.1768 Ma|||Unconformably underlain by Killi Killi Formation. Unconformably overlain by Gardiner Sandstone.|Thickly bedded quartz arenite, lithic arenite, conglomerate, minor siltstone. Interbedded quartz-rich to lithic sandstone, conglomerate and minor siltstone.|
14884|Parker Range Banded Iron Formation|42703|5|Briefly described|map legend|Archean||Reserved as Parker Range BIF.||||||07-NOV-08
14884|Parker Range Banded Iron Formation|43097|4|Described|p10|||||||||
14908|Parnell Quartz Monzonite|24197|5|Briefly described|p109|Paleoproterozoic|Paleoproterozoic|Of the Bridget Suite. Age: ~1731+/-10Ma. Geological province: Pilbara Block.||||||07-FEB-11
14908|Parnell Quartz Monzonite|41561|3|Fully described|p535|||||||||
14908|Parnell Quartz Monzonite|44152|5|Briefly described|p175|||Of Goode et al.(1988). A small pluton ~50 km E of Nullagine|1731 +/- 14 Ma (Rb-Sr isochron; Goode et al.,1988)||||Hornblende adamellite.|
14908|Parnell Quartz Monzonite|50435|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Age: 1731 +/- 14Ma (Rb-Sr). Geological Province: Kimberley Block. Of the Bridget Suite.||||||07-NOV-08
14908|Parnell Quartz Monzonite|63866|5|Briefly described|p144|Statherian|Orosirian|Eastern Pilbara Craton. Sampled at Granite Hills Well by Nelson (2002) who dated the sample. A Rb-Sr whole-rock age of 1731 +/- 14 Ma is provided from Collins et al., 1988.|1803 +/- 19 Ma (Nelson, 2002)|Bridget Suite||||
14908|Parnell Quartz Monzonite|65008|6|Mentioned|p25|Proterozoic|Proterozoic|Named by Collins et al. (1988).||||||
14908|Parnell Quartz Monzonite|65827|5|Briefly described|p42-43|Statherian|Orosirian|Of Bridget Suite. SHRIMP U-Pb zircon date on hornblende-biotite quartz monzodiorite of 1803+/-19 Ma (Nelson, 2002).||||||
14908|Parnell Quartz Monzonite|66217|5|Briefly described|p55.|Statherian|Orosirian||1803 +/- 19 Ma (SHRIMP U-Pb zircon: Nelson 2002c)|Unit in Bridget Suite.|||Hornblende-biotite quartz monzodiorite.|
14987|Peawah Granodiorite|22906|5|Briefly described|p45, p46 Fig.1|Archean|Archean|Age: 2948+/-5Ma (Nelson 1996).  Geological Province: Mallina Basin (Pilbara Craton).||||||07-NOV-08
14987|Peawah Granodiorite|22953|6|Mentioned|Fig1p3|||||||||
14987|Peawah Granodiorite|23244|6|Mentioned|Fig.2 p22,23||Archean|Age: intrusion at 2948+/-5Ma.||||||07-NOV-08
14987|Peawah Granodiorite|23348|5|Briefly described|220 Fig. 3|Archean|Archean|~2950Ma||||||07-NOV-08
14987|Peawah Granodiorite|23598|4|Described|p12|Archean|Archean|Age: c.2950 Ma.||||||07-NOV-08
14987|Peawah Granodiorite|23743|4|Described|p10|Archean|Archean|Age: c.2950 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
14987|Peawah Granodiorite|23784|5|Briefly described|p32|Archean|Archean|Age: c.2950Ma.||||||07-NOV-08
14987|Peawah Granodiorite|23789|5|Briefly described|p6 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
14987|Peawah Granodiorite|23793|4|Described|p32|Archean|Archean|Age: c.2950Ma.  Intrudes the De grey Group. Geological Province: Pilbara Craton||||||07-NOV-08
14987|Peawah Granodiorite|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province Pilbara Craton.||||||07-NOV-08
14987|Peawah Granodiorite|23936|5|Briefly described|p7, Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age ca. 2948 Ma.||||||07-NOV-08
14987|Peawah Granodiorite|24166|5|Briefly described|p3|||||||||
14987|Peawah Granodiorite|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Age: ca. 2950 Ma. Geological Province: Mallina basin||||||07-NOV-08
14987|Peawah Granodiorite|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 2950 Ma||||||07-NOV-08
14987|Peawah Granodiorite|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Mallina Basin. Age: ca. 2950 Ma (Smithies, pers. Commun. 2000)||||||07-NOV-08
14987|Peawah Granodiorite|30766|6|Mentioned|p21|||||||||
14987|Peawah Granodiorite|39697|4|Described|p49|||||||||
14987|Peawah Granodiorite|42231|6|Mentioned|Fig.1 P328|||||||||
14987|Peawah Granodiorite|43821|5|Briefly described|map legend|Archean|Archean|2948+/-5 Ma. Of Pilbara Supergroup||||||07-NOV-08
14987|Peawah Granodiorite|44150|5|Briefly described|p130-131 Fig.2-130, p147 Tb.2-21, p152|||200 sq. km.|||||Foliated hornblende granodiorite.|
14987|Peawah Granodiorite|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
14987|Peawah Granodiorite|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
14987|Peawah Granodiorite|50370|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton. Age: c. 2950 Ma||||||07-NOV-08
14987|Peawah Granodiorite|61267|5|Briefly described|p71, p73 Tb.1|Archean|Archean|Intrudes the Mallina Formation and Constantine Sandstone. Intrudes by Satirist Granite. Age: c. 2950 Ma. Hornblende-(biotite) tonalite to trondhjemite. Geological Province: Pilbara Craton.||||||07-NOV-08
14987|Peawah Granodiorite|63372|4|Described|Map Legend|Archean|Archean|Geological Province: Mallina Basin and east Pilbara. Age: 2948Ma. Hornblende-biotite high Mg diorite, granodiorite, and tonalite; metamorphosed.||||||07-NOV-08
14987|Peawah Granodiorite|63441|5|Briefly described|p11 Tb. 2, p37|Archean|Archean|Of Indee Suite (Sisters Supersuite). Age: 2948+/-5Ma. Geological province: Pilbara Craton. One of best examples of this supersuite.  Intrudes De Grey Supergroup.||||||07-FEB-11
14987|Peawah Granodiorite|64580|4|Described|map legend||Mesoarchean|Of Indee Suite. Hornblende-biotite high-Mg diorite, granodiorite and tonalite; metamorphosed.||||||09-DEC-08
14987|Peawah Granodiorite|67201|4|Described|p22 Fig.13, p60-61|||In De Grey Superbasin; Mallina Basin. c. 2950 Ma. Geochemically subdivided into Peawah Granodiorite (east) and Peawah Granodiorite (west).|(west) 2948+/-5 Ma, GSWA 118967, Nelson 1997b|||Intrudes Constantine Sandstone, forming contact areole.|Sanukitoids.|
14987|Peawah Granodiorite|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 Indee Suite.|||Hornblende-biotite high-Mg diorite, granodiorite and tonalite; metamorphosed|
14987|Peawah Granodiorite|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin. Isotopic age: shown on legend as c. 2950 Ma.|2948+/-5 Ma (isotopic age, Nelson 1997)||||Metamorphosed hornblende-biotite high-Mg diorite, granodiorite, and tonalite|02-SEP-14
14987|Peawah Granodiorite|69590|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological province: Pilbara Craton, West Australian Craton. Events: Pilbara Craton breakup; North Pilbara Orogeny.||Unit of Indee Suite.|||Hornblende-biotite high-Mg diorite, granodiorite and tonalite; metamorphosed|
14987|Peawah Granodiorite|70775|6|Mentioned|p63, p65, p78-p79|Mesoarchean|Mesoarchean|This is the largest intrusion of the Indee Suite underlying an area of 180 km ^2 and is a composite body that can be divided into an eastern and western part.|c. 2948 Ma|Indee Suite||||
14987|Peawah Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, tonalite, diorite|
14987|Peawah Granodiorite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean||2948+/-5 Ma.|Indee Suite|||Hornblende--biotite granodiorite and tonalite; metamorphosed.|
15013|Peepingee Greensand Member|23726|5|Briefly described|p82|||Of Nanutarra Formation. Geological Province: Carnarvon Basin.||||||
15013|Peepingee Greensand Member|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15013|Peepingee Greensand Member|39158|6|Mentioned|p37|||||||||
15013|Peepingee Greensand Member|39427|4|Described|Table 1|||||||||
15013|Peepingee Greensand Member|41271|3|Fully described|p143|||||||||
15013|Peepingee Greensand Member|42116|4|Described|p63|||See also Fig.25||||||
15013|Peepingee Greensand Member|42598|4|Described|P 36|||of Nanutarra Formation||||||
15026|Pelsart Limestone|23816|6|Mentioned|p256|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
15026|Pelsart Limestone|36257|6|Mentioned|Table 2.1|||||||||
15026|Pelsart Limestone|36890|5|Briefly described|p256|||||||||
15034|Pender Bay Conglomerate|23722|4|Described|p36|Tertiary|Tertiary|Geological Province: Canning Basin||||||
15034|Pender Bay Conglomerate|30897|5|Briefly described|p19|||||||||
15034|Pender Bay Conglomerate|30898|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15034|Pender Bay Conglomerate|32648|6|Mentioned|p32|||Tertiary||||||
15034|Pender Bay Conglomerate|36257|6|Mentioned|Table 2.1|||||||||
15034|Pender Bay Conglomerate|36890|4|Described|p355|||||||||
15034|Pender Bay Conglomerate|42814|5|Briefly described|p24|||||||||
15034|Pender Bay Conglomerate|42815|5|Briefly described|map|Cenozoic||||||||19-NOV-08
15034|Pender Bay Conglomerate|44998|2|Defined|p196, 195||Cenozoic|Overlies Broome Sandstone & Jowlaenga Formation. Overlain by Borda Sandstone.||||||19-NOV-08
15034|Pender Bay Conglomerate|45153|2|Defined|App.10-155|early Tertiary|early Tertiary|||||||
15034|Pender Bay Conglomerate|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fluviatile ferruginous boulder conglomerate|
15043|Pentecost Sandstone|22440|6|Mentioned|p5|||||||||
15043|Pentecost Sandstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.||||||07-NOV-08
15043|Pentecost Sandstone|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Kimberley Group.||||||
15043|Pentecost Sandstone|23383|4|Described|p19, p18 Tb. 2|||Of Kimberley Group. Fine- to medium-grained sandstone, coarse-grained quartz sandstone, pebble and cobble conglomerate, siltstone, mudstone.  Conformably overlies Elgee Siltstone. Max. thickness: 900 m.  Geological Province: Kimberley Basin.||||||25-JAN-05
15043|Pentecost Sandstone|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Kimberley Group.  Divided into upper,  middle and lower units of various grades of sandstone and siltstone. Geological Province: Kimberley Basin.||||||21-JUL-15
15043|Pentecost Sandstone|23722|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Parent: Kimberley Group.   Max. thickness: 1375m.   Geological Province: Kimberley Basin||||||07-NOV-08
15043|Pentecost Sandstone|23806|5|Briefly described|p1122|||Geological Province: Kimberley Basin.||||||
15043|Pentecost Sandstone|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Sandstone, pebbly sandstone, siltstone and shale.  Geological Province: Kimberley Basin.||||||07-NOV-08
15043|Pentecost Sandstone|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Age: <1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
15043|Pentecost Sandstone|29693|6|Mentioned|p100|||||||||
15043|Pentecost Sandstone|29946|6|Mentioned|p253|||||||||
15043|Pentecost Sandstone|30097|6|Mentioned|Table 23|||Also Tables 24,29||||||
15043|Pentecost Sandstone|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|30533|4|Described|p18|||On Table 3.||||||
15043|Pentecost Sandstone|30893|5|Briefly described|p205|||Carpentarian. Lithology||||||
15043|Pentecost Sandstone|30894|5|Briefly described|p250|||Carpentarian||||||
15043|Pentecost Sandstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|30896|4|Described|p17|||||||||
15043|Pentecost Sandstone|30897|6|Mentioned|p14|||On stratigraphic table||||||
15043|Pentecost Sandstone|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15043|Pentecost Sandstone|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
15043|Pentecost Sandstone|31662|6|Mentioned|p255|||||||||
15043|Pentecost Sandstone|32660|5|Briefly described|Table 3|||||||||
15043|Pentecost Sandstone|32662|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|32663|4|Described|Table 1|||Capentarian||||||
15043|Pentecost Sandstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
15043|Pentecost Sandstone|32728|6|Mentioned|Table 5|||||||||
15043|Pentecost Sandstone|33443|6|Mentioned|p260|||||||||
15043|Pentecost Sandstone|33540|6|Mentioned|p890|||||||||
15043|Pentecost Sandstone|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|34115|6|Mentioned|p384|||||||||
15043|Pentecost Sandstone|34137|4|Described|Table 1||Carpentarian|Carpentarian. Part of Kimberley Group.||||||
15043|Pentecost Sandstone|34190|4|Described|Table 1|||||||||
15043|Pentecost Sandstone|34462|4|Described|Table 1|||Carpentarian||||||
15043|Pentecost Sandstone|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15043|Pentecost Sandstone|36003|6|Mentioned|p1028|||||||||
15043|Pentecost Sandstone|36551|4|Described|p32|||||||||
15043|Pentecost Sandstone|36885|4|Described|p185|||||||||
15043|Pentecost Sandstone|36902|6|Mentioned|p11|||||||||
15043|Pentecost Sandstone|37228|6|Mentioned|Fig.2|||||||||
15043|Pentecost Sandstone|37462|6|Mentioned|Fig.4.9|||||||||
15043|Pentecost Sandstone|37577|6|Mentioned|p32|||||||||
15043|Pentecost Sandstone|38482|6|Mentioned|Table 1|||||||||
15043|Pentecost Sandstone|39116|6|Mentioned|p134|||||||||
15043|Pentecost Sandstone|41158|6|Mentioned|p24|||||||||
15043|Pentecost Sandstone|41453|6|Mentioned|p242|||||||||
15043|Pentecost Sandstone|41703|6|Mentioned|Fig.2|||||||||
15043|Pentecost Sandstone|41987|5|Briefly described|Fig.4 P74|||||||||
15043|Pentecost Sandstone|42149|6|Mentioned|Table 1 P709|||||||||
15043|Pentecost Sandstone|42190|6|Mentioned|p269|||||||||
15043|Pentecost Sandstone|42710|5|Briefly described|map legend|Proterozoic||||||||
15043|Pentecost Sandstone|42811|5|Briefly described|p23|||of Kimberley Group||||||
15043|Pentecost Sandstone|42814|4|Described|p14|||of Kimberley Group||||||
15043|Pentecost Sandstone|42815|5|Briefly described|map|Proterozoic||||||||
15043|Pentecost Sandstone|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Group.||||||
15043|Pentecost Sandstone|43652|5|Briefly described|Fig.5,p383|||||||||
15043|Pentecost Sandstone|43666|6|Mentioned|p51,Table 2||Neoproterozoic|||||||
15043|Pentecost Sandstone|44140|5|Briefly described|p294-295, p298 fig 4-5|Paleoproterozoic|Paleoproterozoic|420 to 1350 m thick.||Kimberley Group||Intruded by Wotjulum Porphyry. Is overlain conformably by Hilfordy Formation (Crowhurst Group) and Mendena Formation (Bastion Group).|Quartz and feldspathic sandstone, ferruginous siltstone and sandstone, glauconitic sandstone; widespread consistent marker beds; cross-beds, clay pellets.|08-MAR-18
15043|Pentecost Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
15043|Pentecost Sandstone|44231|5|Briefly described|Map Legend||Proterozoic|Of Kimberley Gp. Comprises upper, middle and lower units: lower quartz sandstone and siltstone; middle white, fine- to coarse-grained qtz sst, purple fine-grained sst and purple sltst and shale; and, upper medium- to coarse-gr. qtz sst and pebblt qtz sst.||||||19-MAY-05
15043|Pentecost Sandstone|44286|5|Briefly described|Map legend|||||||||
15043|Pentecost Sandstone|44363|5|Briefly described|p.15,16,27|||(Carpentarian) Kimberley Group.||||||
15043|Pentecost Sandstone|44364|14|Not recorded|map legend|||||||||
15043|Pentecost Sandstone|44366|14|Not recorded|p.16, Table 2||Carpentarian|Part of Kimberley Group.||||||
15043|Pentecost Sandstone|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Kimberley Group.||||||
15043|Pentecost Sandstone|44397|14|Not recorded|p.17, Table 2||Carpentarian|Kimberley Group.||||||
15043|Pentecost Sandstone|44398|14|Not recorded|map legend||Carpentarian|||||||
15043|Pentecost Sandstone|44694|5|Briefly described|Map Legend||Proterozoic|||||||
15043|Pentecost Sandstone|45047|5|Briefly described|p28|||Kimberley Group.||||||
15043|Pentecost Sandstone|45077|6|Mentioned|p7|||||||||
15043|Pentecost Sandstone|48931|3|Fully described|p55|||||||||
15043|Pentecost Sandstone|60714|5|Briefly described|p112, p113 Fig.2, p118. |Statherian|Statherian|c.1000 m thick. Age by McNaughton et al. (1999).|1704 +/- 14 Ma (U-Pb diagenetic xenotime).|Topmost unit in Kimberley Group.||Overlies Elgee Siltstone.|Mature, quartzose and feldspathic sandstone; includes rounded 1mm grains of glauconite.|
15043|Pentecost Sandstone|61571|5|Briefly described|p656, p657 Fig. 4|Paleoproterozoic|Paleoproterozoic|Divided into Middle and Lower units (Fig. 3, p656). Youngest unit in Spider impact structure.  Fine- to coarse-grained, mature and partly quartzitic arenite. Overlies Elgee Siltstone.  Age: 1704+/-14Ma. Max. thickness :600m. Geol.Prov: Kimberley Basin.||||||07-NOV-08
15043|Pentecost Sandstone|64580|4|Described|map legend||Paleoproterozoic|Of Kimberley Group. Sandstone, pebbly sandstone, siltstone, and shale.||||||09-DEC-08
15043|Pentecost Sandstone|64748|4|Described|p269 Fig 2, Tb.1, p268, 271-275, 277-278|Statherian|Orosirian|of Kimberley Group; contains red beds used for palaeomag studies; Conformably overlies Elgee Sandstone; intruded by Hart Dolerite; diagenetic xenotime age 1704+/-14Ma; Youngest detrital zircon 1800Ma(?); informally divided into upper, middle, lower members; quartzose to feldspathic sst; ~420-1350+m thick||||||
15043|Pentecost Sandstone|67269|5|Briefly described|p20-21 Fig.19|Statherian|Statherian|Montgomery Reef. A sample labelled ?Pentecost Sandstone 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).|1704 +/- 14 Ma.|Kimberley Group.||||
15043|Pentecost Sandstone|67563|5|Briefly described|p120, p121, p130, p131|Statherian|Orosirian|Youngest detrital zircon age by Kirkland et al. (2010). Diagenetic xenotime age of 1704 +/- 14 Ma by McNaughton et al. (1999). Two additional youngest detrital zirocn ages are also included.|1796 +/- 24 Ma (maximum deposition).|Of the Kimberley Group.||Intruded by the Hart Dolerite.||20-JAN-17
15043|Pentecost Sandstone|68078|6|Mentioned|p4 figure 2, p6 figure 3, p7-8|Paleoproterozoic|Paleoproterozoic|Age is of approximate depositional age. See also p19, p21 figure 14.|1704 +/- 14 Ma (SHRIMP)|Kimberley Group||Overlies Elgee Siltstone, Warton Sandstone, overlain by Yampi Formation. Intruded by Hart Dolerite|Sandstone.|13-SEP-22
15043|Pentecost Sandstone|68244|6|Mentioned|p666|||Kimberley Basin. Records glacially striated pavement is preserved.||Unit of Kimberley Group.||Overlain unconformably by Landrigan Formation (Kuniandi Group).||21-JUN-19
15043|Pentecost Sandstone|68992|5|Briefly described|p498, p498 Fig.1, p499, pp504-507|Statherian||Kimberley Basin. Diagenetic xenotime age of 1704 +/- 14 Ma (McNaughton et al. 1999). Youngest detrital zircon age.|1796 +/- 24 Ma (Kirkland et al, 2010f).|Of the Kimberley Group.||Underlain by the King Leopold Sandstone. Intruded by the Hart Dolerite.||
15043|Pentecost Sandstone|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic||1704 Ma (U-Pb xenotime age).|Kimberley Group.||Overlies Elgee Siltstone. Is overlain by Yampi Formation.||
15043|Pentecost Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. Max age from data released June 2012, geochron file 109639.1.pdf. Xenotime overgrowths on zircon grains indicate a depositional or diagenetic age of 1704 +/- 14 Ma, considered a minimum age for the unit. See geochron file 82104.1.pdf.|Max.deposit 1774+/-9 Ma U/Pb SHRIMP|Uppermost Kimberley Group|Includes 3 unnamed members|Underlain by Elgee Siltstone. Overlain by Neoproterozoic glacigene sequences.|Quartz sandstone, pebbly sandstone, siltstone, and mudstone|21-JUL-15
15043|Pentecost Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.||Kimberley Group|||Medium to coarse grained quartz sandstone and pebbly quartz sandstone, pink and white quartz sandstone, purple to grey fine grained sandstone and purple siltstone and mudstone. Feldspathic sandstone and micaceous siltstone.|
15043|Pentecost Sandstone|69585|4|Described|p3-5, p8-9, p12, p17, p22-29|Statherian|Orosirian|U-Pb and Lu-Hf isotope data and diagram. A maximum depositional age of 1862 +/- 5 Ma was obtained for the upper [sic] part of the Formation.|1796 +/- 16 Ma (maximum depositional age).|Uppermost Kimberley Group.||Overlies Elgee Siltstone conformably or Warton Sandstone unconformably. Is overlain unconformably by the Bastion and Mount House Groups.|Medium- to coarse-grained quartz sandstones, overlain by cupriferous and ferruginous sandstone, siltstone and shale, topped by a succession coarsening upward into sandstone and pebbly sandstone.|
15043|Pentecost Sandstone|69597|6|Mentioned|p4|||||||||
15043|Pentecost Sandstone|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Thickness: 1000-1600m. Weighted mean 207Pb*/206Pb* ages include 1862+\-5, 1796+\-24 Ma (interpreted maximum depositional ages; various geochron files). Includes xenotime overgrowths on zircon grains at 1704+\-14 Ma, indicating depositional or diagenetic age (Griffin et al., 1993). Minimum depositional age of 1740+\-6 Ma, based on magmatic crystallisation age of Wotjulum Porphyry that intrudes Elgee Siltstone. Contains detrital zircons with max depositional ages of 1862+\-5 Ma (GSWA 182101, Kirkland et al., 2010a) and 1796+\-24 Ma (182102, Kirkland et al., 2010b). Contain zircon age components at c. 1900-1800 and 2500-2400 Ma (McNaughton et al., 1999; Kirkland et al., 2010). Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.  See1 00k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1835-1740 Ma (Inferred)|Unit of Kimberley Group.||Underlain by Elgee Siltstone.|Medium- to coarse-grained quartz and feldspathic sandstone and pebbly quartz sandstone, micaceous siltstone and mudstone|
15043|Pentecost Sandstone|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, Kimberley Craton.||Unit in Kimberley Group.|||Quartz sandstone, pebbly sandstone, siltstone and claystone (section only); lower unit: quartz sandstone, feldspathic sandstone, and micaceous siltstone.|
15043|Pentecost Sandstone|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin; North Australian Craton.||Kimberley Group.||Overlies Elgee Siltstone.|Quartz sandstone, pebbly sandstone, siltstone and claystone.|
15043|Pentecost Sandstone|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Upper Kimberley Group.||Overlies Elgee Siltstone.|Quartz sandstone, pebbly sandstone, siltstone and claystone; a lower unit, separately mapped, of quartz sandstone, feldspathic sandstone, and micaceous siltstone.|
15043|Pentecost Sandstone|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1740-1835 Ma|Kimberley Group|||Quartz sandstone, pebbly sandstone, siltstone, and claystone. Medium to coarse grained quartz sandstone and pebbly quartz sandstone.|
15043|Pentecost Sandstone|70731|5|Briefly described|p270|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||Unit of Kimberley Group.||||
15043|Pentecost Sandstone|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.||Overlies Elgee Siltstone.|Quartz sandstone, pebbly sandstone, siltstone and claystone. An un-named lower unit of quartz sandstone, feldspathic sandstone, and micaceous siltstone, is mapped separately.|
15043|Pentecost Sandstone|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. Mapped as three un-named sub-units.||Kimberley Group.||Overlies Elgee Siltstone.|Quartz sandstone, feldspathic sandstone, and micaceous siltstone; overlain by pink and white quartz sandstone, purple to grey fine-grained sandstone, purple siltstone and mudstone; then medium- to coarse-grained sandstone and pebbly quartz sandstone.|
15043|Pentecost Sandstone|70812|5|Briefly described|p6|Statherian|Statherian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1800 Ma|Kimberley Group, Upper||||
15043|Pentecost Sandstone|70851|5|Briefly described|p4, p6, p34-p35|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1775-1750 Ma|Kimberley Subgroup, Upper||Overlies the Elgee Sandstone.||
15043|Pentecost Sandstone|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological provice: Halls Creek Orogen; King Leopold Orogen. Of Kimberley Basin. Thickness: 1000-1600m. 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, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files. Depositional or diagenetic age of 1704+\-14 Ma (xenotime; McNaughton et al., 1999).|1835-1740 Ma (inferred)|Unit of Kimberley Group.||Underlain by Elgee Siltstone. Intruded by Wotjulum Porphyry.|Blocky medium-grained quartz sandstone, minor fine- to medium-grained feldspathic sandstone; micaceous and glauconitic sandstone, shale pellet conglomerate|
15043|Pentecost Sandstone|71281|4|Described|p421, p423|Paleoproterozoic|Paleoproterozoic|Gellatly and Derrick (1967). Kimberley Basin. Up to 1400m thick. c.1704 Ma age from metamorphic xenotime.|1806 +/- 28 Ma (maximum depositional age).|Kimberley Group.||Overlies Elgee Siltstone.|Blocky, medium-grained quartz sandstone, minor fine- to medium-grained feldspathic sandstone, micaceous and glauconitic sandstone, shale-pellet conglomerate.|
15043|Pentecost Sandstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. The three facies are mapped separately.||Kimberley Group.|||Lower: quartz, feldspathic sandstones, micaceous siltstone. Middle: pink and white quartz sandstone, purple to grey fine-grained sandstone, purple siltstone and mudstone. Upper: medium- to coarse-grained quartz, pebbly quartz sandstones.|
15043|Pentecost Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group, upper|||Quartz sandstone, pebbly sandstone, siltstone, and claystone.|
15043|Pentecost Sandstone|72490|5|Briefly described|p3|||Maximum thickness of 1400 m.||Kimberley Group|||Medium-grained quartz sandstone with interbeds of fine-grained to medium-grained feldspathic sandstone, micaceous and glauconitic sandstone, shale-pellet conglomerate.|
15071|Peron Sandstone|11797|5|Briefly described|map legend|Pleistocene|Pleistocene|Shark Bay Area.|||||Red, quartzose sandstone; common soil structures; eolian.|
15071|Peron Sandstone|23726|5|Briefly described|p8 Fig 2c|Quaternary|Pliocene|Overlying unit Dampier Limestone. Underlying unit Trealla Limestone. Geological Province: Carnarvon Basin.||||||
15071|Peron Sandstone|23815|4|Described|p305|Early Pleistocene|Pliocene|Geological Province: Carnarvon Basin. Overlying unit: Tamala Eolianite. Max. thickness: 122 m.||||||14-DEC-04
15071|Peron Sandstone|31949|5|Briefly described|p62|||||||||
15071|Peron Sandstone|32750|5|Briefly described|p312|||||||||
15071|Peron Sandstone|35105|6|Mentioned|Fig.3|||||||||
15071|Peron Sandstone|36890|3|Fully described|p305|||||||||
15071|Peron Sandstone|38485|4|Described|p18|||||||||
15071|Peron Sandstone|38493|6|Mentioned|p38|||||||||
15071|Peron Sandstone|38494|6|Mentioned|p30|||||||||
15071|Peron Sandstone|40336|6|Mentioned|p19|||||||||
15071|Peron Sandstone|40340|6|Mentioned|p16|||||||||
15071|Peron Sandstone|40342|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15071|Peron Sandstone|40343|5|Briefly described|p15|||||||||
15071|Peron Sandstone|40617|6|Mentioned|p18|||||||||
15071|Peron Sandstone|41271|3|Fully described|p196|||||||||
15071|Peron Sandstone|41438|6|Mentioned|Fig.23|||||||||
15071|Peron Sandstone|42116|5|Briefly described|Fig.1 P6|||||||||
15071|Peron Sandstone|43256|6|Mentioned|20||Early Pleistocene|||||||
15071|Peron Sandstone|45142|6|Mentioned|p27|||||||||
15071|Peron Sandstone|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Pindilya Formation, Trealla Limestone, overlain by Dampier Limestone, Tamala Limestone|Planar cross bedded sandstone.|
15071|Peron Sandstone|69558|4|Described|p27 fig 33, p28 fig 34, p66, 103-106|Pleistocene|Pleistocene|Type locality at Cape Peron is 120m thick. Outcrops discontinuously along the shorelines of the Peron Peninsula and Faure Island. Is considered to be an eolianite. Is distinguished from the Tamala Limestone by its lack of cross-bedding. See also p70 fig 102, p73 fig 107, p95, p98, p103-106, p113, p248 fig 404, p249, p260, p262.|||Includes the Hoult Sandstone Member.|Is laterally equivalent to the Tamala Limestone with which it interfingers. Overlain by the Denham Sand.|Red, poorly bedded, partly calcareous sandstone.|25-MAY-21
15071|Peron Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
15094|Pertatataka Formation|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale.||||||
15094|Pertatataka Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|22560|5|Briefly described|p2|||||||||
15094|Pertatataka Formation|22561|4|Described|p24|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22562|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|22564|5|Briefly described|p59||Neoproterozoic|||||||
15094|Pertatataka Formation|22566|5|Briefly described|p73|Neoproterozoic|Neoproterozoic|In the north of the Ooraminna depocentre, the Pertatataka Fromation overlies the lower subunits of the Olympic Formation at this Type Section - p81.||||||
15094|Pertatataka Formation|22567|5|Briefly described|p91|||Age: 730+/-45 Ma Rb-Sr data (Compston and Taylor, 1969).||||||04-SEP-14
15094|Pertatataka Formation|22646|4|Described|p 99|Neoproterozoic|Neoproterozoic|informal name - lower Pertatataka Formation is mentioned on p 101||||||
15094|Pertatataka Formation|22649|5|Briefly described|p 152|Neoproterozoic|Neoproterozoic|Underlain by Gaylad Sandstone.||||||22-NOV-06
15094|Pertatataka Formation|22651|6|Mentioned|Fig 10 btw p182-183|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22652|6|Mentioned|p 222|||||||||
15094|Pertatataka Formation|22653|6|Mentioned|Fig 14 on p 236|||||||||
15094|Pertatataka Formation|22746|5|Briefly described|p513, p529|||||||||
15094|Pertatataka Formation|22761|6|Mentioned|p358|||||||||
15094|Pertatataka Formation|22762|5|Briefly described|p378|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22763|5|Briefly described|p398|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22804|6|Mentioned|p440|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22805|5|Briefly described|p464|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22823|4|Described|p517-518|Proterozoic|Proterozoic|||||||
15094|Pertatataka Formation|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|22901|6|Mentioned|78|||Geological  province: Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|22921|6|Mentioned|39|||Geological province: Amadeus Basin.||||||17-APR-13
15094|Pertatataka Formation|23250|5|Briefly described|p1124  Fig.2||Neoproterozoic III|Correlate of Tent Hill Formation and Yarloo Shale, and Bunyeroo Formation, ABC Range Quartzite and Brachina Formation.||||||
15094|Pertatataka Formation|23282|6|Mentioned|p89|||In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23287|6|Mentioned|p104 Fig.4|||Age: Ediacarian. In the Amadeus Basin.||||||22-NOV-06
15094|Pertatataka Formation|23314|5|Briefly described|333 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
15094|Pertatataka Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|Age: ~600Ma.||||||22-NOV-06
15094|Pertatataka Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|24064|5|Briefly described|p229 Fig.7|Adelaidean|Adelaidean|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. See also p215 Fig. 11.||||||
15094|Pertatataka Formation|24301|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin||||||
15094|Pertatataka Formation|24442|6|Mentioned|p38|||Geological Province: Centralian Superbasin.||||||
15094|Pertatataka Formation|29721|6|Mentioned|Table 44|||||||||
15094|Pertatataka Formation|29972|6|Mentioned|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|30220|6|Mentioned|p244|||||||||
15094|Pertatataka Formation|30258|6|Mentioned|Fig.2|||About 730m.y.||||||
15094|Pertatataka Formation|30544|6|Mentioned|p48|||On map legend||||||
15094|Pertatataka Formation|31026|6|Mentioned|p61|||||||||
15094|Pertatataka Formation|31566|6|Mentioned|p230|||Proterozoic||||||
15094|Pertatataka Formation|31645|6|Mentioned|Table 2|||Correlation||||||
15094|Pertatataka Formation|32144|6|Mentioned|p81|||Organic matter||||||
15094|Pertatataka Formation|32376|6|Mentioned|p1541|||||||||
15094|Pertatataka Formation|32442|6|Mentioned|p9|||||||||
15094|Pertatataka Formation|32469|6|Mentioned|p531|||||||||
15094|Pertatataka Formation|32720|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
15094|Pertatataka Formation|33025|6|Mentioned|p928|||Minimum age 800 m.y.||||||
15094|Pertatataka Formation|33102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|33103|6|Mentioned|p23|||||||||
15094|Pertatataka Formation|33630|6|Mentioned|p906|||||||||
15094|Pertatataka Formation|33655|6|Mentioned|p101|||||||||
15094|Pertatataka Formation|33761|6|Mentioned|p146|||Adelaidean. Contains Olympic Member||||||
15094|Pertatataka Formation|34111|4|Described|Table 1|||Precambrian. See also Table 4, pp11,14,17,19.||||||22-NOV-06
15094|Pertatataka Formation|34186|6|Mentioned|Fig.3|||Late Precambrian. See also Fig.4.||||||
15094|Pertatataka Formation|34202|6|Mentioned|p1058|||||||||
15094|Pertatataka Formation|34287|6|Mentioned|p41|||See also p42.||||||22-NOV-06
15094|Pertatataka Formation|34442|5|Briefly described|Table 1|||Proterozoic||||||
15094|Pertatataka Formation|34488|4|Described|Table 1|||Proterozoic. See also pp10,14,16.||||||22-NOV-06
15094|Pertatataka Formation|34579|5|Briefly described|Table 1|||See also pp15,17, Fig.2.||||||22-NOV-06
15094|Pertatataka Formation|34580|4|Described|Table 1|||||||||
15094|Pertatataka Formation|35064|6|Mentioned|p208|||||||||
15094|Pertatataka Formation|35088|6|Mentioned|p92|||||||||
15094|Pertatataka Formation|35102|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|35136|6|Mentioned|p140|||||||||
15094|Pertatataka Formation|35798|6|Mentioned|p307|||||||||
15094|Pertatataka Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
15094|Pertatataka Formation|35863|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|36198|6|Mentioned|Fig.III.2|||||||||
15094|Pertatataka Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15094|Pertatataka Formation|36898|6|Mentioned|p198|||||||||
15094|Pertatataka Formation|37371|6|Mentioned|p382|||||||||
15094|Pertatataka Formation|37462|4|Described|Table 4.IX|||||||||
15094|Pertatataka Formation|37572|6|Mentioned|p153|||||||||
15094|Pertatataka Formation|37928|6|Mentioned|p517|||||||||
15094|Pertatataka Formation|37929|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|38157|6|Mentioned|Table VI|||||||||
15094|Pertatataka Formation|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|38945|6|Mentioned|p134|||||||||
15094|Pertatataka Formation|39210|4|Described|p37|||||||||
15094|Pertatataka Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
15094|Pertatataka Formation|39558|6|Mentioned|Table 2|||||||||
15094|Pertatataka Formation|39565|6|Mentioned|p32|||||||||
15094|Pertatataka Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated siltstone and shale, sandstone. Geological Province: Amadeus Basin.||||||14-FEB-06
15094|Pertatataka Formation|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15094|Pertatataka Formation|40105|6|Mentioned|p311|||||||||
15094|Pertatataka Formation|40201|5|Briefly described|Table 1|||||||||
15094|Pertatataka Formation|40740|3|Fully described|p12|||||||||
15094|Pertatataka Formation|40810|6|Mentioned|p3|||||||||
15094|Pertatataka Formation|40852|6|Mentioned|p29|||||||||
15094|Pertatataka Formation|40856|5|Briefly described|p316|||||||||
15094|Pertatataka Formation|41005|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41039|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41115|6|Mentioned|p1389|||||||||
15094|Pertatataka Formation|41190|6|Mentioned|Fig.4|||||||||
15094|Pertatataka Formation|41203|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|41224|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41270|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|41429|5|Briefly described|p246|||||||||
15094|Pertatataka Formation|41618|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|41717|5|Briefly described|p355|||||||||
15094|Pertatataka Formation|41801|6|Mentioned|p218|||||||||
15094|Pertatataka Formation|41852|6|Mentioned|p209|||||||||
15094|Pertatataka Formation|42059|6|Mentioned|Fig.2 P131|||||||||
15094|Pertatataka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
15094|Pertatataka Formation|42082|6|Mentioned|Fig.3 P323|||||||||
15094|Pertatataka Formation|42504|5|Briefly described|p72|||||||||
15094|Pertatataka Formation|42643|6|Mentioned|Fig.4 P19|||||||||
15094|Pertatataka Formation|42845|6|Mentioned|Fig.3 P498|||||||||
15094|Pertatataka Formation|42886|4|Described|p223|||see also Fig.2 p219.||||||22-NOV-06
15094|Pertatataka Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Shale, siltstone.  Geological province: Amadeus Basin.||||||04-SEP-14
15094|Pertatataka Formation|43011|6|Mentioned|Table 2,p12|||||||||
15094|Pertatataka Formation|43057|5|Briefly described|p68|||||||||
15094|Pertatataka Formation|43105|5|Briefly described|Fig.3,p8|||||||||
15094|Pertatataka Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
15094|Pertatataka Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
15094|Pertatataka Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
15094|Pertatataka Formation|43622|6|Mentioned|p39|||||||||
15094|Pertatataka Formation|43647|6|Mentioned|Fig.4,533|||||||||
15094|Pertatataka Formation|43648|6|Mentioned|p491|||||||||
15094|Pertatataka Formation|43649|5|Briefly described|p457|||||||||
15094|Pertatataka Formation|43756|6|Mentioned|p542|||||||||
15094|Pertatataka Formation|43817|6|Mentioned|Fig.1,p42|||||||||
15094|Pertatataka Formation|44261|14|Not recorded|p7-19|||Not recorded on white card.||||||
15094|Pertatataka Formation|44262|14|Not recorded|p3-21|||Not listed on white card.||||||
15094|Pertatataka Formation|44335|4|Described|p.7||Proterozoic|Tb.1. p.8.||||||
15094|Pertatataka Formation|44342|14|Not recorded|p.5|||SG/53-5, correlated with Winnall Beds.||||||
15094|Pertatataka Formation|44395|14|Not recorded|p.6|||Correlates with Ellis Sandstone and Maurice Formation.||||||22-NOV-06
15094|Pertatataka Formation|44402|5|Briefly described|map legend||Proterozoic|||||||02-DEC-04
15094|Pertatataka Formation|44433|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44484|14|Not recorded|p.10, Fig.4, Tb.1||Proterozoic|||||||
15094|Pertatataka Formation|44485|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44497|4|Described|p.6, Table 1||Proterozoic|SF/53-13.||||||
15094|Pertatataka Formation|44498|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|44505|14|Not recorded|p.7, Fig.1, Table 1||Proterozoic|||||||
15094|Pertatataka Formation|44506|14|Not recorded|map legend||Proterozoic|||||||
15094|Pertatataka Formation|45041|4|Described|p32|||Proterozoic||||||
15094|Pertatataka Formation|45052|6|Mentioned|p67|||||||||
15094|Pertatataka Formation|45079|6|Mentioned|p16|||||||||
15094|Pertatataka Formation|46730|5|Briefly described|p7|||Underlain by Pioneer Sandstone. Geological Province: Amadeus Basin||||||22-NOV-06
15094|Pertatataka Formation|46829|6|Mentioned|Fig.2|||||||||
15094|Pertatataka Formation|46865|4|Described|p51|||||||||
15094|Pertatataka Formation|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
15094|Pertatataka Formation|46928|6|Mentioned|Table 1|||||||||
15094|Pertatataka Formation|47035|6|Mentioned|Fig.1|||||||||
15094|Pertatataka Formation|48639|14|Not recorded|p.13,opp.p.1||Neoproterozoic|See also page, 11. Pl.2,Sh.2. U.Prot. (G55-2,15,G53-3).||||||
15094|Pertatataka Formation|48838|2|Defined|p.13, Tb.1|||||||||
15094|Pertatataka Formation|48844|14|Not recorded|p.8|||||||||
15094|Pertatataka Formation|48862|14|Not recorded|p.8|||On many pages. p.1,8,13,16,18,21,34,38,41,43; opp.8,9; Pl.2,7,10. (F52-15).||||||
15094|Pertatataka Formation|48863|2|Defined|p.12|||Tb.1. opp.p.7,9,11,17,38-40, Pl.15,16. ?Upper Proterozoic, or Lower Cambrian. (G52-4,G53-1).||||||
15094|Pertatataka Formation|48864|14|Not recorded|Tb.1,p.1,26,31|||||||||
15094|Pertatataka Formation|48865|14|Not recorded|Fig.4,p.20,45|||(F53-13).||||||
15094|Pertatataka Formation|48880|14|Not recorded|p.20,20,33,Pl.10-13||Neoproterozoic|U.Prot. 750 m.y. (F53-13,14).||||||
15094|Pertatataka Formation|48890|4|Described|p.22-31|||See also Tables, Figs and Plates. Includes: Ringwood Member, Olympic Member, Limbla Member, Julie Member, Cyclops Member. Defn on Tech.File F/53-13.||||||22-NOV-06
15094|Pertatataka Formation|48963|6|Mentioned|p5|||||||||
15094|Pertatataka Formation|48990|6|Mentioned|p11|||||||||
15094|Pertatataka Formation|49796|5|Briefly described|Sect C BDF 28|||||||||
15094|Pertatataka Formation|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Includes the Cyclops Member.||||||07-FEB-11
15094|Pertatataka Formation|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and shale with lenses of sandstone, limestone, dolomite, conglomerate. Geological Province: Amadeus Basin.||||||07-JUN-05
15094|Pertatataka Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains the Waldo Pedlar Member.  Laminated siltstone and shale, some sandstone.||||||02-FEB-05
15094|Pertatataka Formation|60674|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|White to yellow-brown, laminated and thinly-bedded fine kaolinitic sandstone with interbeds of laminated micaceous siltstone.  Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone; limestone with stromatolites. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated and thin-bedded, fine kaolinitic sandstone, with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||04-OCT-05
15094|Pertatataka Formation|61518|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded fine grained kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Laminated and thin bedded, fine kaolinitic sandstone with interbeds of micaceous siltstone. Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|61732|3|Fully described|p4 Fig. 3, p94-95|Marinoan|Marinoan|Formerly incl. six members: Limbla and Ringwood Members and Olympic and Julie "Members" all now redefined; but retains Cyclops and Waldo Pedlar Members. Max. thickness: 570m. Geol.Prov: Amadeus Basin. See also p5 Tb. 1.||||||10-SEP-14
15094|Pertatataka Formation|62085|6|Mentioned|p15 Fig.1, p20  |||Amadeus Basin. Contains distinctive acritarch assembly: Appendisphaera barbata.|||||Marine siltstone.|
15094|Pertatataka Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15094|Pertatataka Formation|62379|5|Briefly described|p7 Fig. 2, p26|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Thickness: 600m. Black shale. Lateral equivalent of Winnall beds.||||||
15094|Pertatataka Formation|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Neoproterozoic III|Palaeomagnetic data.||||||10-FEB-09
15094|Pertatataka Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Amadeus Basin.||||||
15094|Pertatataka Formation|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||Includes Cyclops Member.||Sandstone, fine-grained, undulose to flat and laminated and fissile.|
15094|Pertatataka Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone, shale, limestone, calcarenite, dolomite, some sandstone and tillitic conglomerate.||||||
15094|Pertatataka Formation|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Pertatataka, and Pertatataka Fm.||||overlies Cap Dolomite; is overlain by Julie Formation.||
15094|Pertatataka Formation|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|Amadeus Basin.||||Is overlain by Julie Formation.||
15094|Pertatataka Formation|63562|5|Briefly described|p338 fig 3, p343, 344, p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin. Coarsens to the S, implying source in Musgrave Inlier.||||Overlies Pioneer Sandstone.|Deep-water turbidites and pelagic sediments.|
15094|Pertatataka Formation|63811|6|Mentioned|p503,505, p519-527 App A|Ediacaran|Ediacaran|Of Amadeus Basin. Has acritarch fossils in common with Ungoolya Group, Officer Basin, and Doushantuo Formation, South China. Also correlated with Khamaka and Kursov Formations, Siberia.||||||28-MAR-12
15094|Pertatataka Formation|64068|6|Mentioned|p49, 51, 224|||Amadeus Basin. Lower part correlated with Gnallan-a-Gea Arkose, Elyuah Formation, medial to upper part with Grant Bluff Formation, southern Georgina Basin.||||||
15094|Pertatataka Formation|64625|5|Briefly described|p243-257|Neoproterozoic|Neoproterozoic|Amadeus Basin. Has a basal "cap carbonate".|||Includes Cyclops Member|Overlies Gaylad Sandstone, Pioneer Sandstone. Is overlain gradationally by Julie Formation.|Siltstone and shale, sandstone.|
15094|Pertatataka Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
15094|Pertatataka Formation|64778|6|Mentioned|p13, 18|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
15094|Pertatataka Formation|64797|5|Briefly described|p152, p153 Fig.2, p157-159 |||See also p164 Fig.11, p167 Tb.10, p168 Tb.11, p176-177. Of Amadeus Basin. S-isotope data.||||Correlated with Brachina Formation (Adelaide Rift Complex).||
15094|Pertatataka Formation|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Proterozoic|Proterozoic|See also p13 Fig.13, p15 Fig.15. Widespread transgressive deposits.|||Includes Cyclops Member.||Fine marine siliciclastics (siltstone, shale).|
15094|Pertatataka Formation|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
15094|Pertatataka Formation|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Formerly Winnall beds. Disconformable on Bitter Springs Fm; disconform.or conform.on Olympic Fm; below Julie Fm. Max.thick: 500m. Amadeus Basin.Thick extensive marine shales in succession of mainly fine-gr.clastics, predom'l red/green shale+ fine-gr. sst||||||07-FEB-11
15094|Pertatataka Formation|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
15094|Pertatataka Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
15094|Pertatataka Formation|65338|5|Briefly described|p64.|||Amadeus Basin. Correlative with Elyuah Formation.|||||Predominantly micaceous siltstone and shale with thinly interbedded sandstone; rare limestone.|
15094|Pertatataka Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 19 m.||||Is overlain by Julie Formation.|Fine kaolinitic sandstone.|
15094|Pertatataka Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Amadeus Basin. Includes Acanthomorph acritarchs.||||||
15094|Pertatataka Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Amadeus Basin||||||
15094|Pertatataka Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3. Contains distinctive, well-documented and well-constrained palynomorph assemblages of biostratigraphic significance, including acritarchs.||||||
15094|Pertatataka Formation|65416|6|Mentioned|p141, p146.|||Amadeus Basin. Tentatively correlated with Boondawari Formation (Officer Basin). Suggested by Perincek (1996) to pre-date the Petermann Ranges Orogeny.||||||
15094|Pertatataka Formation|65489|5|Briefly described|p125|Proterozoic|Proterozoic|Amadeus Basin.||||Overlies Aralka Formation. Is overlain by Arumbera Formation.||
15094|Pertatataka Formation|65892|6|Mentioned|p35.|Late Neoproterozoic|Late Neoproterozoic|Amadeus Basin. Contains same acritarchs as Bunyeroo and lower Wonoka Formations, Adelaide Geosyncline.||||||
15094|Pertatataka Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. 350m thick in its type section; locally up to 1400m thick. Deep-water, pelagic deposits.|||||Predominantly red and green siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|67326|4|Described|p2, p7-10, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. Intersected by stratigraphic drillhole BRD05DD01. Over 450m thick. South of the Angas Lineament Zone (previously the Central Ridge), the Winnall beds are widespread and 400-500m thick; the authors state that the term is redundant, and the rocks subsumed into the Pertatataka Formation. Probable source of gas in the Dingo gas field; a potential source rock for dry gas over wide areas of the Basin. Rockeval Pyrolysis results discussed. Core section photographs. Composite log.||||Conformably to disconformably overlies Olympic or Bitter Springs Formations. Is overlain by Julie Formation.|Red-brown to occasionally grey siltstone and mudstone, becoming evaporitic towards the top. Occasional upward-fining cycles representing turbidity current deposits.|
15094|Pertatataka Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation. Underlain by the Olympic Formation.||
15094|Pertatataka Formation|67565|5|Briefly described|p5 Fig.3, p39, p46.|Ediacaran|Ediacaran|Amadeus Basin. Deep water siliciclastic sediments. Forms strike ridges. 350 m thick, increasing to the west.||||Is overlain unconformably by the Arumbera Sandstone.|White to yellow-brown, laminated and thinly-bedded, fine-grained kaolinitic sandstone; poorly exposed interbeds of laminated micaceous siltstone.|
15094|Pertatataka Formation|67620|6|Mentioned|p5, 22|Ediacaran|Ediacaran|Amadeus Basin. Contains abundant organic laminae (microbial mats).||||Overlies Olympic Formation. Is overlain by Julie Formation.||
15094|Pertatataka Formation|67856|5|Briefly described|p338 fig 4-30, p337, p345 |Neoproterozoic|Neoproterozoic|||||Underlain by Olympic Formation.||
15094|Pertatataka Formation|67912|6|Mentioned|p12, 25-27|||Amadeus Basin. Contains diverse assemblages of complex, large acritarchs.||||||
15094|Pertatataka Formation|68270|5|Briefly described|p679,683-684|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone and Olympic Formation.||
15094|Pertatataka Formation|68271|6|Mentioned|p696|||Adelaide Rift Complex.||||||
15094|Pertatataka Formation|68275|6|Mentioned|p61|||Variations in the Ediacaran sulfur-isotope record world-wide are briefly discussed.||||||
15094|Pertatataka Formation|68276|6|Mentioned|p71, 73-74|||Amadeus Basin. The ""Formation"" is omitted.",,||||Conformably overlies Olympic Formation.|Reddish-grey laminated siltstone with limestone turbidites.|
15094|Pertatataka Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15094|Pertatataka Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
15094|Pertatataka Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran|Ediacaran|Amadeus Basin.||||||
15094|Pertatataka Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
15094|Pertatataka Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Pioneer and Gaylad Sandstones. Is overlain by Julie Formation.|Siltstone and shale.|12-JUL-16
15094|Pertatataka Formation|69438|2|Defined|p23:2-5, 7-8, 10, 17-21, 27,43,47, 59-60|Ediacaran|Ediacaran|Pritchard and Quinlan (1962). The type section is 5km W of Ellery Creek and c.350m thick. Originally defined with two clastic units separated by a dolomite layer. Only the lower clastic unit remains to constitute the Formation; the other units are now the Olympic and Julie Formations. Amadeus Basin. Up to 1400m thick. Generally recessive; the Cyclops Member forms low ridges in places. Previously correlated with Winnall beds, but that unit is now correlated with Carnegie Formation and Arumbera Sandstone. One of the most likely oil- and/or gas-prone units in the Basin. Thick shales form seals over older reservoirs.|||Cyclops, Waldo Pedlar Members.|Disconformably overlies Olympic Formation, Pioneer Sandstone or Bitter Springs Formation. Is overlain conformably by Julie Formation.|Mainly (320m) red and green siltstone and shale, with flaser bedding, small-scale cross-laminations and thin interbeds of fine-grained sandstone; overlain by 1.5m of grey medium-grained feldspathic silicified sandstone and 30m of red siltstone.|12-JUL-16
15094|Pertatataka Formation|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
15094|Pertatataka Formation|69606|4|Described|p1, p4 fig 2, p5, p6 fig 3, p7 fig 4, |Early Ediacaran|Early Ediacaran|c. 300m thick. Potential source and seal rock. Amadeus Basin. Type area In north-central Amadeus Basin mentioned. Contact with the Julie Formation is poorly exposed. See also  p14, p15 fig 8, p16, p18, p19.||||Overlies the Pioneer Sandstone and the Olympic Formation. Conformably (gradational) overlain by the Julie Formation.|Red and green siltstone, shale and minor sandstone.|
15094|Pertatataka Formation|69673|5|Briefly described|p63, p74, p80, p81, p86, p88, p90, p97,|Neoproterozoic|Neoproterozoic|Up to 1400m thick. Potential source rock and unconventional gas potential.|||Includes Cyclops Member, Waldo Pedlar Member|Overlain by Julie Formation, conformably overlies Gaylad Sandstone, overlies Pioneer Sandstone, correlated with Winnall beds|Siltstone, shale and feldspathic sandstone.|
15094|Pertatataka Formation|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p14, p20, p23|Neoproterozoic|Neoproterozoic|See also p25-31, p51-54. Amadeus Basin. Inferred depositional age of ~575 Ma.|||Cyclops, Waldo Pedlar Members.|Overlies Olympic Formation unconformably and Gaylad Sandstone conformably. Is overlain conformably by Julie Formation.|Mainly grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Julie Formation. Underlain by Pioneer Sandstone.||
15094|Pertatataka Formation|70416|5|Briefly described|p63-65, p80|Ediacaran|Ediacaran|Amadeus Basin. Earlier definitions included rocks subsequently assigned to Aralka Formation.|||Waldo Pedlar, Cyclops Members.|Overlies Olympic Formation and Pioneer Sandstone. Is overlain by Julie Formation.||
15094|Pertatataka Formation|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.|||Includes Gaylad Sandstone.|Overlain by Julie Formation. Underlain by Olympic Formation or Pioneer Sandstone.||
15094|Pertatataka Formation|71001|5|Briefly described|p18 Fig.2, p20, 23, 27-28|Ediacaran|Ediacaran|Amadeus Basin. Marine deposits. Carbon isotope correlation graph.|||Waldo Pedlar, Cyclops Members.|Overlies Gaylad Sandstone. Is overlain by Julie Formation.|Dominantly marine pyritic shale.|
15094|Pertatataka Formation|71080|6|Mentioned|p29 fig 20, p30, 31|Ediacaran|Ediacaran|Amadeus Basin. Supersequence 3. Probable source rock for Dingo Field in eastern Amadeus.|||||Dominantly shale in WA. Includes carbonate and sandstone in NT.|
15094|Pertatataka Formation|71088|5|Briefly described|p2, p8, p15|lower Ediacaran|lower Ediacaran|Northern and eastern Amadeus Basin. The lower part of this formation was correlated with the Ellis Sandstone, Sir Frederick Conglomerate and the Maurice Formation by Wells et al., 1970; Grey, 1990; Lindsay and Korsch, 1991.||||||
15094|Pertatataka Formation|71279|5|Briefly described|p353, p355 Fig.2, p365-368, p370, p382|Ediacaran|Ediacaran|Amadeus Basin. Contains interbedded reduced and oxidised iron-rich layers. Contains zircons aged c.1.3 to 0.8 Ga sourced from Tjauwata Group (Musgrave Province). Magnetisation discussed in detail. Modelled magnetic properties.|||||Highly weathered grey-green shale and salty dolomite.|
15094|Pertatataka Formation|71288|6|Mentioned|p146|||Implications of a c.540 Ma paleopole position from this unit discussed.||||||
15094|Pertatataka Formation|71344|4|Described|p1092, 1094, 1095, 1096-1103|Ediacaran||Amadeus Basin. Includes acritarch assemblages that give depositional age constraints (Zhou et al., 2007). Deposited under marine conditions. 300-550 m thick.|635 - 582 Ma|Of Pertaoorta Package.|Includes Waldo Pedlar Member, Cyclops Member.|Conformably overlies the Olympic Formation, Gaylad Sandstone and is succeeded by the Julie Formation.|Red, green to dark green shales and siltstones. Lower and middle part dominated by laminated, dark grey, pyritic siltstone and shale.|10-NOV-17
15094|Pertatataka Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71801|6|Mentioned|p230-p231|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by the Julie Formation.||
15094|Pertatataka Formation|71810|5|Briefly described|Map legend.|Ediacaran|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Siltstone, shale, and minor sandstone; very poorly exposed.|
15094|Pertatataka Formation|71841|5|Briefly described|p1-2,13|Ediacaran|Ediacaran|Of Amadeus Basin. Original stratigraphy based on McKinnon-Matthews (2009): CPD003: 181.3-219m EOH. Revised stratigraphy in drill core: not intersected.|||Includes Cyclops and Waldo Pedlar members.|Overlain by Julie Formation. Underlain by Pioneer Sandstone or Gaylad Sandstone. Grades into Inindia beds.||
15094|Pertatataka Formation|71842|5|Briefly described|p1-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).|||Includes Cyclops Member and Waldo Pedlar Member.|Overlain by Julie Formation. Underlain unconformably by Olympic/Pioneer Formation. Correlable with Winnall beds.||
15094|Pertatataka Formation|71898|5|Briefly described|p6|||Amadeus Basin.||||Unconformably (possibly) overlain by the Quandong Conglomerate.||
15094|Pertatataka Formation|72360|5|Briefly described|Solid Geology map|||Of Amadeus Basin.||||||
15094|Pertatataka Formation|72369|4|Described|iii,p3-4,11,14-p15|||Of Amadeus Basin. Originally of Pritchard and Quinlan, 1962. Maidment (2005) provided an inferred depositional age of 575 Ma; further inferred age constraint provided by its stratigraphic position above the Gaylad Sandstone that was deposited during the c. 640-580 Ma Elatina Glaciation (Walter et al 1995). LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND364 (very coarse- to coarse grained sandstone) yielded an interpreted maximum depositional age of 822+\-11 Ma (youngest concordant zircon) does not further constrained the depositional age of the Pertatataka Formation as it is significantly older than the 575 Ma inferred depositional age of Maidment (2005). Contains significant proportion of detrital zircons derived from Musgrave Province (between c. 1500 Ma and c. 970 Ma age spectrum), and Aileron and Warumpi provinces (c. 1810 to c. 1625 Ma age spectrum), and minor Archean-Plaeoproterozoic (>c. 1780 Ma) and Neoproterozoic zircons indicate potential distal sources from the Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.|||Includes Waldo Pedlar and Cyclops members.|Overlain by Winnall Group. Overlies the Gaylad Sandstone.|Red and green siltstone, shale, and fine to medium-grained feldspathic sandstone. Fine to medium-grained, red-brown quartz sandstone.|18-DEC-19
15094|Pertatataka Formation|72374|5|Briefly described|p14|||Of Amadeus Basin. Provenance spectra of Waldo Pedlar Member dominated by Musgrave Province-sourced zircon with lesser zircon sourced from Aileron and Warumpi provinces.|||Includes Waldo Pedlar Member.|||11-OCT-19
15094|Pertatataka Formation|72375|4|Described|p1-2,19-20,23,25,27,29,31|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Pritchard and Quinlan 1962. Intepreted maximum depositional age of c. 575 Ma (Maidment 2005). Deep water depositional environment.|||Includes Waldo Pedlar Member, Cyclops Member.|Overlain conformably by Julie Formation. Underlain unconformably by Gaylad Sandstone.|Grey-green and purple-brown laminated, micaceous siltstone and shale with thin interbeds of sandstone and limestone.|
15094|Pertatataka Formation|72489|6|Mentioned|p4 Fig.3, p4|Ediacaran|Ediacaran|Located in the Amadeus Basin.|>548.8 +/- 1 Ma|||Overlain by Julie Formation.||
15094|Pertatataka Formation|72516|6|Mentioned|p88-89|Ediacaran|Ediacaran|Amadeus Basin.|||Includes the Cyclops Member.|Lower part equivalent to the Elyuah Formation. Cyclops Member equivalent to Grant Bluff Formation.||02-JUN-21
15094|Pertatataka Formation|72601|5|Briefly described|p3-4, p7-9, p11-12, p17, p25|Ediacaran|Ediacaran|Amadeus Basin. Preiss et al. (1978) subdivided the original Pertatataka Formation into five formations; Aralka Formation, Olympic Formation (former Olympic Member), Pioneer Sandstone, the revised Pertatataka Formation, and Julie Formation.||||Underlain by Olympic Formation and Pioneer Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73085|4|Described|piii, p1, p3, p15-16, p18-19, p26-27|Ediacaran|Ediacaran|Amadeus Basin. Lithology is here described from a 136-metre-thick equivalent in drillhole BR05DD01. Sharp contact with underlying Aralka Formation marked by abrupt lithological change.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Aralka Formation, Pioneer Sandstone [/ Olympic Formation] and Gaylad Sandstone. Overlain by Julie Formation. Equivalent to Inindia beds.|Red-brown calcareous siltstone and fine-grained sandstone, micaceous, becoming green-grey siltstone with fine-grained sandstone intervals, calcareous.|
15094|Pertatataka Formation|73086|1|Redefined|[See comments].|Ediacaran|Ediacaran|[Defined herein. No revised definition card]. Post-glacial transgressive unit. Characterised by red and green siltstone with localised conglomerate. Amadeus Basin. Part of Supersequence III. Named was first used by Madigan (1932) from a dictionary of the Arunta language meaning red rock. Type section: Ellery Creek. Key locality: Olympic Bore. Distribution: extends across most of the eastern and central parts of the basin although it is generally poorly exposed (typically only several metres thick); exposures are best in the northeast. Type section thickness: 350 m. Maximum thickness: 1800 m. Originally included several units that were later separately defined such as Ringwood Member, Limbla Member, Aralka Formation, Olympic Formation, Julie Formation. Undivided Pertatataka Formation siltstones referred to as lower, middle or upper Pertatataka Formation according to position relative to formal members, or as undivided Pertatataka Formation where specific level is uncertain or referring to the unit as a whole. Can be difficult to distinguish the unit from siltstones of the Aralka Formation and non-diamictite lithologies of the Olympic Formation. No known macrofossils; large sphaeromorph and acanthomorph acritarch assemblages found in this unit; used to correlate with Rodda beds. Inferred depositional age of 575 Ma (Maidment, 2005). A detrital zircon maximum depositional age of ca 807 Ma is significantly older than the inferred true depositional age. Thinly bedded siltstone represents a quiet, marine depositional setting. Also correlates to Rodda beds, Elyuah Formation, Grant Bluff Formation, Gnallan-a-gea Arkose, Cox Formation, Bukalara Formation, Buckingham Bay Sandstone, Raiwalla Shale, Mount Doreen Formation, Bunyeroo Formation, Brachina Formation, ABC Range Quartzite. p: 3, 5-6, 53, 71-72, 75, 78-79, 90-91, 99-101, 107, ~113-118, 121-135, 143, 160, 163-169, 171.|ca 570 Ma||Cyclops Member, Waldo Pedlar Member|Conformably underlain by Pioneer Sandstone, Olympic Formation, Gaylad [Sandstone]. Overlain by Julie Formation. Correlates to upper Inindia beds and more [see comments].|Red and green siltstone with lenticular bedding, small-scale cross-laminations, and thin interbeds of sandstone overlain by grey, medium-grained, silicified, feldspathic sandstone, which in turn is overlain by red siltstone with sandstone laminae.|
15094|Pertatataka Formation|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.|||Cyclops Member, Waldo Pedlar Member|Unconformably underlain by Pioneer Sandstone and Gaylad Sandstone. Overlain by Julie Formation.||
15094|Pertatataka Formation|73180|4|Described|p47-49, p51 Fig.6, p52|Neoproterozoic|Neoproterozoic|Amadeus Basin.|||Cyclops Member and Waldo Pedlar Members|Conformably overlies the Olympic Formation and Pioneer Sandstone, conformably underlies the Julie Formation.|Primarily red, brown and green shales, siltstones and fine sandstones.|
15094|Pertatataka Formation|73279|5|Briefly described|p3, p6-7|Ediacaran|Ediacaran|Amadeus Basin, eastern. Detrital zircons analysed for Hf isotopic composition [see article].||||May be equivalent to Gloaming Formation.|Includes sandstone.|
15099|Pertnjara Group|9199|5|Briefly described|Map legend|Devonian|Devonian|Includes the Brewer Conglomerate and Hermannsburg Sandstone.  Geological Province: Amadeus Basin.||||||04-NOV-04
15099|Pertnjara Group|9814|5|Briefly described|Map Legend|Devonian|Devonian|||||||
15099|Pertnjara Group|22560|5|Briefly described|p3|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22561|4|Described|p26||Early Devonian|||||||
15099|Pertnjara Group|22564|4|Described|p60||Devonian|Min age - ? Carboniferous.  Underlain by Mereenie Sandstone.||||||22-NOV-06
15099|Pertnjara Group|22566|5|Briefly described|p84|Carboniferous|Early Devonian|||||||12-APR-12
15099|Pertnjara Group|22646|6|Mentioned|p 105|||||||||
15099|Pertnjara Group|22650|5|Briefly described|p 165|Carboniferous|Devonian|||||||
15099|Pertnjara Group|22651|6|Mentioned|Fig 10 btw p182-183||Devonian|||||||
15099|Pertnjara Group|22655|5|Briefly described|p 255|||||||||
15099|Pertnjara Group|22656|6|Mentioned|p 277||Devonian|||||||
15099|Pertnjara Group|22657|6|Mentioned|p 297|Devonian|Devonian|||||||
15099|Pertnjara Group|22760|4|Described|p333-337|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|22761|6|Mentioned|p350|Late Devonian|Early Devonian|||||||
15099|Pertnjara Group|22762|5|Briefly described|p377||Devonian|Distal equivalent to the Finke Group p376.||||||
15099|Pertnjara Group|22763|6|Mentioned|p394||Late Devonian|||||||
15099|Pertnjara Group|22804|4|Described|p442|Carboniferous|Middle Devonian|||||||
15099|Pertnjara Group|22805|5|Briefly described|p465||Middle Devonian|||||||
15099|Pertnjara Group|22807|6|Mentioned|Fig 3 on p495|||Age - (?)Middle Devonian-(?)Late Devonian.||||||
15099|Pertnjara Group|22824|5|Briefly described|p525|||||||||
15099|Pertnjara Group|23282|6|Mentioned|p83|||May correlate with Mimili Formation. In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|23361|5|Briefly described|15|Devonian|Devonian|||||||
15099|Pertnjara Group|23732|5|Briefly described|p31|Late Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|23858|5|Briefly described|p913|Devonian||Underlain by Mereenie Sandstone. Geological Province: Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|24063|5|Briefly described|p220|Early Carboniferous|Late Devonian|Geological Province: Amadeus Basin. Maximum thicknes: 3650m.||||||
15099|Pertnjara Group|24064|5|Briefly described|p229 Fig.7|Carboniferous|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|24111|6|Mentioned|p214 Fig. 9|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|29442|6|Mentioned|p103|||||||||
15099|Pertnjara Group|29721|6|Mentioned|Table 44|||||||||
15099|Pertnjara Group|29807|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29817|6|Mentioned|p13|||||||||
15099|Pertnjara Group|29972|6|Mentioned|p4|||Devonian-Carboniferous||||||
15099|Pertnjara Group|30238|4|Described|p68|||Upper Devonian to Carboniferous age||||||
15099|Pertnjara Group|30258|6|Mentioned|Fig.2|||Devonian - ?Carboniferous||||||
15099|Pertnjara Group|30544|6|Mentioned|p51|||||||||
15099|Pertnjara Group|30659|6|Mentioned|p87|||||||||
15099|Pertnjara Group|31566|4|Described|p230|||See also p231. Refers Wells et al. (1970).||||||22-NOV-06
15099|Pertnjara Group|31567|6|Mentioned|p273|||Refers Finke Group.||||||22-NOV-06
15099|Pertnjara Group|31707|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|31991|4|Described|p294|||Struct. geol. and geol.history.||||||22-NOV-06
15099|Pertnjara Group|32208|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
15099|Pertnjara Group|32640|6|Mentioned|p235|||||||||
15099|Pertnjara Group|32865|6|Mentioned|p482|||||||||
15099|Pertnjara Group|33103|6|Mentioned|p25|||||||||
15099|Pertnjara Group|33306|6|Mentioned|p206|||||||||
15099|Pertnjara Group|33307|6|Mentioned|Fig.6|||||||||
15099|Pertnjara Group|33326|6|Mentioned|p449|||Fauna.||||||
15099|Pertnjara Group|33761|6|Mentioned|p146|||Devonian - Carb?||||||
15099|Pertnjara Group|33971|6|Mentioned|p30|||Refers stratigraphy.||||||
15099|Pertnjara Group|34111|5|Briefly described|Table 2|||Devonian - Carboniferous. See also pp5,6,14,16.||||||22-NOV-06
15099|Pertnjara Group|34186|6|Mentioned|Fig.3|||Devonian - Permian. See also Figs 4,8.||||||
15099|Pertnjara Group|34442|5|Briefly described|Table 1|||Devonian - Carboniferous||||||
15099|Pertnjara Group|34579|4|Described|Table 3|||Devonian - Carboniferous. See also pp16,17.||||||22-NOV-06
15099|Pertnjara Group|34580|4|Described|Table 1|||||||||
15099|Pertnjara Group|34810|6|Mentioned|p9|||Re ages.||||||
15099|Pertnjara Group|35102|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|35628|6|Mentioned|Table 3|||||||||
15099|Pertnjara Group|36473|6|Mentioned|Map legend|Carboniferous|Devonian|Between Carboniferous and Devonian||||||
15099|Pertnjara Group|38319|6|Mentioned|p328|||||||||
15099|Pertnjara Group|38606|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|39213|6|Mentioned|p15|||Molasse conglomerate. Fig.6||||||
15099|Pertnjara Group|39565|6|Mentioned|Fig.14|||||||||
15099|Pertnjara Group|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15099|Pertnjara Group|40201|5|Briefly described|p691|||||||||
15099|Pertnjara Group|40740|3|Fully described|p60|||Briefly described p6.||||||22-NOV-06
15099|Pertnjara Group|40810|5|Briefly described|p12|||||||||
15099|Pertnjara Group|40906|6|Mentioned|Fig.11|||||||||
15099|Pertnjara Group|41018|6|Mentioned|p234|||||||||
15099|Pertnjara Group|41039|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41125|6|Mentioned|p40|||See also fig.24.||||||
15099|Pertnjara Group|41190|6|Mentioned|p267|||||||||
15099|Pertnjara Group|41204|6|Mentioned|p14|||||||||
15099|Pertnjara Group|41224|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41270|6|Mentioned|p268|||||||||
15099|Pertnjara Group|41385|6|Mentioned|p363|||See also Fig.12||||||
15099|Pertnjara Group|41492|6|Mentioned|p158|||||||||
15099|Pertnjara Group|41708|6|Mentioned|Fig.1|||||||||
15099|Pertnjara Group|41717|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|41723|6|Mentioned|Map legend|Late Devonian||||||||
15099|Pertnjara Group|41820|6|Mentioned|p6|||See also Fig.3||||||
15099|Pertnjara Group|42060|6|Mentioned|Fig.5 P140|||||||||
15099|Pertnjara Group|42141|6|Mentioned|Fig.3 P570|||||||||
15099|Pertnjara Group|42351|6|Mentioned|p46|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42354|6|Mentioned|p7|||||||||
15099|Pertnjara Group|42504|6|Mentioned|p80|||||||||
15099|Pertnjara Group|42564|6|Mentioned|p12|||In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|42643|6|Mentioned|p32|||||||||
15099|Pertnjara Group|42699|5|Briefly described|map legend|Devonian||||||||
15099|Pertnjara Group|42845|5|Briefly described|p496|||||||||
15099|Pertnjara Group|42940|5|Briefly described|Plate 2|Devonian|Devonian|Sandstone, siltstone, conglomerate, limestone; fish fossils.  Age: 410-360Ma. Geological province: Amadeus Basin.||||||23-JAN-08
15099|Pertnjara Group|43035|4|Described|p23|||||||||
15099|Pertnjara Group|43105|5|Briefly described|Fig.3,p8.|||||||||
15099|Pertnjara Group|43225|5|Briefly described|Map Legend||Devonian|In the Amadeus Basin.||||||22-NOV-06
15099|Pertnjara Group|43503|6|Mentioned|32-50|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|43631|6|Mentioned|p27|||||||||
15099|Pertnjara Group|43646|6|Mentioned|p553||Devonian|||||||
15099|Pertnjara Group|43647|6|Mentioned|p530|||||||||
15099|Pertnjara Group|43648|5|Briefly described|Fig.1,p488|||||||||
15099|Pertnjara Group|43649|5|Briefly described|fig.1,p454-455,459|||||||||
15099|Pertnjara Group|43749|6|Mentioned|p37|||||||||
15099|Pertnjara Group|43817|6|Mentioned|Fig.1,p62|||||||||
15099|Pertnjara Group|44133|5|Briefly described|p44|Devonian|Devonian|Includes: Parke Siltstone.||||||
15099|Pertnjara Group|44342|4|Described|p.6, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
15099|Pertnjara Group|44343|14|Not recorded|map legend|Carboniferous|Devonian|Dev. to Carbon.||||||
15099|Pertnjara Group|44393|6|Mentioned|p.6,7,8,Fig.1|||Correlated with Finke Group.||||||
15099|Pertnjara Group|44395|14|Not recorded|p.9,10,12, Tb.2|||Devonian?||||||
15099|Pertnjara Group|44402|5|Briefly described|map legend|Carboniferous|Devonian|Includes Hermannsburg Sandstone and Parke Siltstone. Dev-Carb.||||||02-DEC-04
15099|Pertnjara Group|44433|14|Not recorded|map legend|||Devonian to Carboniferous.||||||
15099|Pertnjara Group|44484|14|Not recorded|p.5,8,9,11,Tb.1,Fig4|Carboniferous|Devonian|Defn on Tech.File F/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44485|14|Not recorded|map legend|Carboniferous|Devonian|Includes Parke Silstone, Hermannsburg Sandstone. Dev-Carb.||||||
15099|Pertnjara Group|44493|4|Described|p.13, map|Carboniferous|Devonian|BLOODS RANGE sheet (G53-3). Dev-Carb.||||||22-NOV-06
15099|Pertnjara Group|44494|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|44495|4|Described|p.9, map|Carboniferous|Devonian|AYERS ROCK sheet (G52-8). Devonian-Carb.||||||22-NOV-06
15099|Pertnjara Group|44496|5|Briefly described|map legend|Carboniferous|Devonian|Red-brown siltstone.  Devonian-Carboniferous.||||||22-NOV-06
15099|Pertnjara Group|44497|4|Described|p.11, Table 2|Carboniferous|Devonian|SF/53-13. Dev-Carb.||||||
15099|Pertnjara Group|44498|14|Not recorded|map legend|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44505|14|Not recorded|p.2,8, Fig.11|Carboniferous|Devonian|Dev-Carb.||||||
15099|Pertnjara Group|44506|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carboniferous.||||||
15099|Pertnjara Group|45041|4|Described|p94|||See also ppP95-102. U.Dev. to L.Carb.||||||22-NOV-06
15099|Pertnjara Group|45097|6|Mentioned|p27|||See also p28. Brachiopods.||||||22-NOV-06
15099|Pertnjara Group|45140|5|Briefly described|p13-14, p64-65|Early Carboniferous|Devonian|Wells et al. (1970). Amadeus Basin. Non-marine: broad alluvial plain deposits. Similar lithology to Pedestal Beds. Equivalent to Angas Hills Beds.|||Parke Siltstone.|Correlated with Lucas Formation.||
15099|Pertnjara Group|45148|6|Mentioned|p20|||||||||
15099|Pertnjara Group|45153|6|Mentioned|p55|||||||||
15099|Pertnjara Group|45155|6|Mentioned|Fig.8|||||||||
15099|Pertnjara Group|45170|6|Mentioned|p9|||||||||
15099|Pertnjara Group|46829|6|Mentioned|Fig.2|||||||||
15099|Pertnjara Group|46830|6|Mentioned|p24|||||||||
15099|Pertnjara Group|46864|6|Mentioned|p40|||||||||
15099|Pertnjara Group|46928|6|Mentioned|Table 1|||||||||
15099|Pertnjara Group|47050|5|Briefly described|p240|||||||||
15099|Pertnjara Group|48890|4|Described|p.49|Carboniferous|Devonian|Ref on wrong card! Pertnjara Formation. See also Tables, Figs and Plates.||||||22-NOV-06
15099|Pertnjara Group|48963|6|Mentioned|p22|||||||||
15099|Pertnjara Group|50246|5|Briefly described|p20 Fig. 2|Carboniferous|Devonian|Includes the N'Dhala Member.||||||07-FEB-11
15099|Pertnjara Group|60547|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Amadeus Basin.||||||03-JUN-05
15099|Pertnjara Group|61154|6|Mentioned|p34|||Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61309|6|Mentioned|p15, p17|Devonian|Devonian|Deposited during the Alice Springs Orogeny. Geological Province: northern margin of Amadeus Basin. See also p25 Fig. 11.||||||06-FEB-08
15099|Pertnjara Group|61387|5|Briefly described|Map legend|Devonian|Silurian|Includes Mereenie Sandstone and undifferentiated rocks.  Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|61519|5|Briefly described|Map Legend|Devonian|Silurian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62359|5|Briefly described|p544 Fig. 4a, p545||Devonian|Foreland basin unit. Geological Province: Amadeus Basin. See also p546 Fig. 6.||||||
15099|Pertnjara Group|62376|5|Briefly described|p18|Late Devonian|Late Devonian|Geological Province: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|62379|5|Briefly described|p7 Fig. 2|Devonian|Devonian|Geological Province: Amadeus Basin.||||||
15099|Pertnjara Group|62595|5|Briefly described|p29 Fig.6.|Carboniferous|Devonian|Ross River area.|||Includes N'Dahla Member.|||
15099|Pertnjara Group|62609|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone. Overlies Mereenie Sandstone.||||||14-AUG-06
15099|Pertnjara Group|62620|5|Briefly described|Map Legend|Carboniferous|Devonian|Sandstone, siltstone, conglomerate, some limestone.||||||
15099|Pertnjara Group|63562|5|Briefly described|p338 fig 3, p352 fig 10, p350|Devonian|Devonian|Of Amadeus Basin. Upward-coarsening lacustrine, fluvial and alluvial fan deposits; thickening northwards.||||Overlies Mereenie Sandstone unconformably. Correlated to Dulcie Sandstone and Ethabuka Sandstone.|Upward-coarsening succession of lacustrine, fluvial and alluvial fan deposits.|
15099|Pertnjara Group|64334|5|Briefly described|p42|Devonian|Devonian|Deposition was synchronous with the main phase of the Alice Springs Orogeny.|||||Thick wedges of generally coarsening-upward non-marine clastic sediments.|
15099|Pertnjara Group|64778|6|Mentioned|p12-13, 33|Devonian|Devonian|N Amadeus Basin margin. Up to 3000m of clastics following the 375-340 Ma Pertnjara Movement (Alice Springs Orogeny).||||||
15099|Pertnjara Group|64809|5|Briefly described|p3, p6 Fig.4 |Late Devonian|Late Devonian||||Includes the Brewer Conglomerate, Hermannsburg Sandstone and Parke Siltstone.|||
15099|Pertnjara Group|64970|6|Mentioned|p719 Fig. 2|Devonian|Silurian|Geological Province: Amadeus Basin.||||||27-MAY-09
15099|Pertnjara Group|65074|6|Mentioned|p360|Devonian|Devonian|Amadeus Basin.||||Probably correlated with Lucas Formation and Pedestal beds (of Birrindudu Basin).||
15099|Pertnjara Group|65232|5|Briefly described|p72, p10 Fig 9.||Late Devonian|Includes Brewer Conglomerate at top. Thick succession of Late Devonian terrestrial sediments. Geol.Prov: Amadeus Basin.||||||09-FEB-10
15099|Pertnjara Group|65233|4|Described|p3 Fig. 2, p13|Late Devonian|Middle Devonian|Unconformable on Mereenie Sandstone. Geological province: Amadeus Basin. Written only as Pertnjara. Upward-coarsening foreland basin succession forming a thick clastic wedge - details incl.||||||07-FEB-11
15099|Pertnjara Group|65272|6|Mentioned|p319, p320 Fig.3|Late Devonian|Late Devonian|Deformed by the Alice Springs Orogeny.||||||
15099|Pertnjara Group|65309|5|Briefly described|p13, p16, pp18-19. |Devonian|Devonian|Central and northern Amadeus Basin. Interfingers with Finke Group. Ongoing uplift resulted in deposition of thicker and more extensive (than Finke Group), upward-coarsening sequence.|||Includes Parkes Siltstone.|||
15099|Pertnjara Group|65342|5|Briefly described|p3.|||Amadeus Basin. Max. thickness at least 194 m.||||Overlies Mereenie Sandstone.|Sandstone, siltstone, conglomerate, some limestone.|
15099|Pertnjara Group|65382|6|Mentioned|p711|Late Devonian|Middle Devonian|||||||
15099|Pertnjara Group|65489|6|Mentioned|p125|Devonian|Devonian|Amadeus Basin.||||||
15099|Pertnjara Group|66498|6|Mentioned|p45|||Amadeus Basin, central Australia.||N'Dhala Member.||||
15099|Pertnjara Group|66589|6|Mentioned|p180|Famennian|Givetian|Case studies cited; not visited in the field by the authors of this study.||||||
15099|Pertnjara Group|66767|5|Briefly described|p60|Devonian|Devonian|Amadeus Basin. Consists of a series of lacustrine, braided and meandering fluviatile and alluvial fan deposits during the Alice Springs Orogeny.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone.||
15099|Pertnjara Group|67326|5|Briefly described|p2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Overlies Larapinta Group.||
15099|Pertnjara Group|67565|5|Briefly described|p5 Fig.3, p42.|||Amadeus Basin.|||Includes Parke Siltstone and Hermannsburg Sandstone.|Overlies Mereenie Sandstone.||03-DEC-15
15099|Pertnjara Group|67856|5|Briefly described|p338, 348|Late Devonian|Late Devonian||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone in N and E of basin.||
15099|Pertnjara Group|68298|6|Mentioned|p226|||Amadeus Basin. Unfossiliferous. Said to be similar age to Aztec Siltstone fauna, Antarctica.||||||
15099|Pertnjara Group|68323|6|Mentioned|p4 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|69031|6|Mentioned|p9|Devonian|Devonian|Eastern Amadeus Basin.||||||
15099|Pertnjara Group|69427|6|Mentioned|p12:47-48|||Amadeus Basin. Synorogenic successions in this unit were progressively tilted as a result of S-directed thrusting in the Devonian.||||||12-JUL-16
15099|Pertnjara Group|69438|4|Described|p23:2-8, 37-40, 42, 46, 48, 50|Famennian|Givetian|Pritchard and Quinlan (1962). Northwest and north-central Amadeus Basin. Thins to the S. Devonian (Givetian- Frasnian)  fish fossils occur at several localities in basal Parke Siltstone. Min age constrained by Famennian spores in Brewer Conglomerate. Deposition was initiated by the Pertnjara Event, and the Group was mildly deformed, uplifted and eroded by the Brewer Event.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|Unconformably overlies Mereenie Sandstone. Correlative of, and interdigitates with, Finke Group.|A series of lacustrine, braided and meandering fluvial, and alluvial fan deposits.|13-SEP-18
15099|Pertnjara Group|69439|5|Briefly described|p24:11-12|Devonian|Devonian|Amadeus Basin. This unit's lithofacies resembles that of the Kerridy Sandstone (Ngalia Basin).|||Brewer Conglomerate.|||12-JUL-16
15099|Pertnjara Group|69449|6|Mentioned|p34:2 Fig.34.2|Devonian|Devonian|Eastern Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69453|6|Mentioned|p37:1|||Amadeus Basin.||||Stratigraphic equivalent to Pedestal beds.||12-JUL-16
15099|Pertnjara Group|69458|6|Mentioned|p42:8|Devonian|Devonian|Amadeus Basin.||||||12-JUL-16
15099|Pertnjara Group|69606|5|Briefly described|p4 fig 2|Carboniferous|Devonian|Deposited during the Alice Springs Orogeny. Amadeus Basin. Potential seal rock.||||Unconformably overlies the Mereenie Sandstone.|Shale, sandstone and conglomerate.|
15099|Pertnjara Group|69673|6|Mentioned|p67, p149 fig 120||||||Includes Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate|Correlated with Finke Group||
15099|Pertnjara Group|69948|6|Mentioned|Fig.4.4|||Amadeus, Georgina and Wiso Basins. Syn-orogenic (Pertnjara Movement/Tabberabberan Orogeny).||||||
15099|Pertnjara Group|71088|6|Mentioned|p17-18|Devonian|Devonian|Amadeus Basin. This unit is locally folded and exposed near the type area of the Ligertwood beds.||||||03-MAY-23
15099|Pertnjara Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15099|Pertnjara Group|71268|5|Briefly described|1m_geologyp12_lut.csv||||||Includes Mereenie Sandstone.|||
15099|Pertnjara Group|71279|5|Briefly described|p355 Fig.2, p363, p374, p382 Tb.1|Late Devonian|Late Devonian|Amadeus Basin. Modelled magnetic properties.|||Parke Siltstone, Hermannsburg Sandstone, Brewer Conglomerate.|||
15099|Pertnjara Group|72360|5|Briefly described|Map legend|Devonian|Devonian|Of Amadeus Basin.|||Includes Brewer Conglomerate.||Includes calcareous siltstone, siltstone, sandstone.|09-SEP-19
15099|Pertnjara Group|72369|5|Briefly described|iii,p40|Late Devonian|Late Devonian|Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72374|5|Briefly described|iii,p3,23|||Of Amadeus Basin.|||Includes Hermannsburg Sandstone.|||
15099|Pertnjara Group|72476|6|Mentioned|p36 Fig.9|||Amadeus Basin. Time-temperature thermal history diagram.||||||
15099|Pertnjara Group|73085|6|Mentioned|p1|late Devonian|late Devonian||||Brewer Conglomerate, Hermannsburg Sandstone, Parke Siltstone|Underlain by Mereenie Sandstone. Equivalent to Finke Group (Larapinta Group).||
15099|Pertnjara Group|73279|6|Mentioned|p14-15|Devonian|Devonian|Amadeus Basin.|||Hermannsburg Sandstone|||
15170|Pidinga Formation|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Of Plantagenet Group. Presented as Pidinga.||||||07-FEB-11
15170|Pidinga Formation|22485|4|Described|p51 , Fig 2 & p53|Tertiary|Tertiary|Informally divided into upper and lower Pidinga Formation.||||||11-JUL-13
15170|Pidinga Formation|22587|6|Mentioned|p79 Fig.7|Middle Eocene|Middle Eocene|||||||
15170|Pidinga Formation|22613|3|Fully described|p19|Late Eocene|Middle Eocene|Eucla Basin.||||||21-OCT-08
15170|Pidinga Formation|22916|5|Briefly described|12|||||||||
15170|Pidinga Formation|23331|5|Briefly described|1088|Late Eocene|Middle Eocene|||||||
15170|Pidinga Formation|23343|5|Briefly described|39|Eocene|Eocene|||||||
15170|Pidinga Formation|23479|5|Briefly described|p26|Paleogene|Paleogene|Geological Province: Gawler Craton [??more likely shown overlying Gawler Craton rocks].||||||04-NOV-10
15170|Pidinga Formation|23488|5|Briefly described|p37, p39 Fig. 5|Middle Eocene|Middle Eocene|Estuarine sand and clay. Geological Province: Eucla Basin.||||||28-JUL-09
15170|Pidinga Formation|23533|5|Briefly described|p564 Fig 3|Late Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23584|5|Briefly described|p31 Fig 17|Late Eocene|Early Eocene|Of Eundynie Group. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23671|2|Defined|p1|Middle Eocene|Middle Eocene|Disconformably overlain by Wilson Bluff Limestone; probably also overlain by Nullarbor Limestone in marginal areas. Max. thickness: 86ft. Type section details included.||||||28-JUL-09
15170|Pidinga Formation|23792|5|Briefly described|Fig.D4|Early Eocene|Late Paleocene|Equivalent to Wobbegong supersequence. Unconformably overlies Potoroo Formation. Overlain by Wilsons Bluff Formation. Geological Province: Bight Basin.||||||21-JAN-16
15170|Pidinga Formation|23818|5|Briefly described|p174 Fig.84|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|23989|5|Briefly described|p54 Fig. 46|Middle Eocene|Early Eocene|Overlies Yilgarn Craton rocks||||||04-NOV-10
15170|Pidinga Formation|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
15170|Pidinga Formation|24201|5|Briefly described|p373 Fig. 2|Ypresian|Thanetian|||||||
15170|Pidinga Formation|24338|5|Briefly described|p938 Fig. 2|Ypresian|Thanetian|Overlain by the Wilson Bluff Limestone and the Nullarbor Limestone. Unconformably overlies the Potoroo Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
15170|Pidinga Formation|24350|5|Briefly described|Fig. 4 Appdx|Ypresian|Thanetian|Equivalent to Wobbegong Supersequence.||||||21-JAN-16
15170|Pidinga Formation|24358|5|Briefly described|p32|Eocene|Eocene|Geological Province: Eucla Basin.||||||17-MAR-05
15170|Pidinga Formation|24396|4|Described|p218 Fig. 3, p221|Late Eocene|Middle Eocene|Lower part correlates with the Maralinga Formation of Clarke et al (2003). Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands. Overlain by Khasta Formation.  Overlies Gawler Craton rocks.||||||04-NOV-10
15170|Pidinga Formation|24397|4|Described|p240|Late Eocene|Late Eocene|Defined by Harris, 1966. Direct equivalent of Werrillup Fm. in WA. Formerly informally divided into upper and lower Pidinga Fm. Upper Pidinga Fm. included here; lower Pidinga Fm. now incl. in Maralinga Fm. Geological Province: Eucla Basin.||||||28-JUL-09
15170|Pidinga Formation|24553|5|Briefly described|p37, Fig. 7|Cenozoic|Cenozoic|Geological Province: Duntroon Sub-basin. Marine sands. Part of Wobbegong Supersequence.||||||07-FEB-11
15170|Pidinga Formation|24606|5|Briefly described|p956, p958 Fig. 3|Late Eocene|Middle Eocene|Geological Province: Eucla Basin||||||
15170|Pidinga Formation|24617|5|Briefly described|p114, p115 Fig. 3, p117, p125 Fig. 10|Eocene|Eocene|Geological Province: Eucla Basin. Conglomerates and sandstones which fine upwards into carbonaceous siltstones, mudstones and lignites.||||||
15170|Pidinga Formation|29591|6|Mentioned|p92|||||||||
15170|Pidinga Formation|29659|6|Mentioned|p8|||||||||
15170|Pidinga Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
15170|Pidinga Formation|30922|6|Mentioned|Map legend|Eocene|Eocene|||||||
15170|Pidinga Formation|31850|3|Fully described|p32|||||||||
15170|Pidinga Formation|32120|6|Mentioned|p276|||Eocene, fauna||||||
15170|Pidinga Formation|32203|6|Mentioned|p5|||Middle Eocene||||||
15170|Pidinga Formation|34308|5|Briefly described|p195|||Johannian||||||
15170|Pidinga Formation|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
15170|Pidinga Formation|35080|6|Mentioned|p8|||||||||
15170|Pidinga Formation|35772|4|Described|Table 1|||||||||
15170|Pidinga Formation|36096|6|Mentioned|p212|||||||||
15170|Pidinga Formation|36213|6|Mentioned|p86|||||||||
15170|Pidinga Formation|37062|6|Mentioned|p187|||||||||
15170|Pidinga Formation|37132|5|Briefly described|p369|||||||||
15170|Pidinga Formation|37852|6|Mentioned|p2|||||||||
15170|Pidinga Formation|38068|5|Briefly described|p73|||See also Fig.7.||||||
15170|Pidinga Formation|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
15170|Pidinga Formation|38602|6|Mentioned|Fig.2|||||||||
15170|Pidinga Formation|38604|6|Mentioned|Map legend|Eocene|Paleocene|Paleocene - Eocene||||||
15170|Pidinga Formation|38605|4|Described|p29|||See also Table 5.||||||
15170|Pidinga Formation|39322|6|Mentioned|Fig.3|||||||||
15170|Pidinga Formation|39923|6|Mentioned|p354|||||||||
15170|Pidinga Formation|39949|5|Briefly described|p274|||||||||
15170|Pidinga Formation|40003|5|Briefly described|Table 14|||||||||
15170|Pidinga Formation|40448|6|Mentioned|p41|||||||||
15170|Pidinga Formation|40912|6|Mentioned|Map legend|late Eocene|late Eocene|Latest Eocene||||||
15170|Pidinga Formation|40941|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15170|Pidinga Formation|41505|6|Mentioned|p2|||||||||
15170|Pidinga Formation|41619|6|Mentioned|Map legend|late Eocene|middle Eocene|||||||
15170|Pidinga Formation|41626|6|Mentioned|p48|||||||||
15170|Pidinga Formation|42075|5|Briefly described|Fig.10 P250|||||||||
15170|Pidinga Formation|42086|3|Fully described|p2|||See also Fig.2.||||||21-OCT-08
15170|Pidinga Formation|42265|6|Mentioned|p2|||||||||
15170|Pidinga Formation|42356|5|Briefly described|Fig.15 P119|Eocene||See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
15170|Pidinga Formation|42465|5|Briefly described|Map Legend|||||||||
15170|Pidinga Formation|42466|5|Briefly described|Map Legend|||||||||
15170|Pidinga Formation|42469|5|Briefly described|p39|||||||||
15170|Pidinga Formation|42475|3|Fully described|p19|||||||||
15170|Pidinga Formation|42545|5|Briefly described|p12|||||||||
15170|Pidinga Formation|42546|5|Briefly described|Map legend|Tertiary||||||||
15170|Pidinga Formation|42722|6|Mentioned|Tectonic sketch legend|Tertiary|Tertiary|||||||
15170|Pidinga Formation|42736|5|Briefly described|map legend|Tertiary||||||||
15170|Pidinga Formation|42816|4|Described|p22|||||||||
15170|Pidinga Formation|42959|5|Briefly described|p56|||see also p58 Fig.3||||||
15170|Pidinga Formation|43071|5|Briefly described|p16,Table 3|||||||||
15170|Pidinga Formation|43280|6|Mentioned|Map Legend||Tertiary|||||||
15170|Pidinga Formation|43814|6|Mentioned|Fig.3,p115|||||||||
15170|Pidinga Formation|43838|4|Described|p4, 9||Tertiary|Interfingers with Hampton Sandstone. Princess Royal Spongolite & Redmine Group overlies. 60m thick.||||||12-JUL-16
15170|Pidinga Formation|44133|5|Briefly described|p178|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Thickness: 60m+.||||||
15170|Pidinga Formation|44145|6|Mentioned|p551  Table 4-27|Eocene|Eocene|Occurs near eastern margin of Eucla Basin in SA.||||Correlated with Hampton Sandstone, Werillip Formation.||
15170|Pidinga Formation|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
15170|Pidinga Formation|44864|5|Briefly described|Map Legend||Eocene|||||||
15170|Pidinga Formation|44935|5|Briefly described|Map Legend|Late Eocene|Middle Eocene|||||||
15170|Pidinga Formation|46993|6|Mentioned|p262|||||||||
15170|Pidinga Formation|49060|5|Briefly described|Fig.15|||||||||
15170|Pidinga Formation|60497|5|Briefly described|p42|Early Oligocene|Eocene|Basal unit in the palaeochannels of the Eucla Basin.  Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|60953|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||11-JUL-13
15170|Pidinga Formation|61108|5|Briefly described|map legend|Eocene|Paleocene|Fluvial to estuarine and marine sand and lignite. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|61155|5|Briefly described|p17|Late Eocene|Middle Eocene|Contains the Bring Member. Interfingers with Wilson Bluff Limestone. Age: ~45-36.5Ma. Max. thickness: 100m. Geological Province: Eucla Basin.||||||
15170|Pidinga Formation|61197|6|Mentioned|p481|Middle Eocene|Middle Eocene|Part of the infill within inset-valleys in the Yilgarn Craton.||||||
15170|Pidinga Formation|61544|5|Briefly described|p367 Fig.3. |Eocene|Paleocene|||||Is overlain by Nullarbor and Wilson Bluff Limestones.|Shallow marine sandstones.|
15170|Pidinga Formation|61630|6|Mentioned|p555 Fig. 3|Paleocene|Late Cretaceous|Geological Province: Bright and Duntroon Basins.||||||07-APR-09
15170|Pidinga Formation|61814|5|Briefly described|p22, p26|Middle Eocene|Middle Eocene|Coarse and fine-grained lignitic and siliciclastic deposit, mainly fluvial and estuarine; carbonaceous. Incised into weathered basement rock of underlying Gawler Craton.||||||04-NOV-10
15170|Pidinga Formation|61839|5|Briefly described|p227|Eocene|Eocene|Mainly fluvial carbonaceous sediments. Overlies Gawler Craton.||||||04-NOV-10
15170|Pidinga Formation|61856|5|Briefly described|p300 Fig.2, p304, p312|Late Eocene|Middle Eocene||||Includes Maralinga and Anthony Members.|||
15170|Pidinga Formation|62570|5|Briefly described|p582|Eocene|Eocene|Sediments overlying Observatory Hill Formation in Wilkinson 1 (core).||||||01-OCT-09
15170|Pidinga Formation|64340|5|Briefly described|p26 Tb. 5, p31|Middle Eocene|Middle Eocene|Of Eundynie Group.||||||
15170|Pidinga Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Oligocene|Eocene|Includes Maralinga and Anthony Members. Geological Province: Gawler Craton.||||||08-FEB-10
15170|Pidinga Formation|65194|5|Briefly described|p136 Fig.4.37, p163-164, p170-172|Middle Eocene|Early Eocene|Oldest sediments in Lefroy Palaeovalley; also occurs in Musgrave region and Gawler Craton. Up to about 50m of fluvial sediments: silt, silty clay, lignite; minor gravel-rich sand bodies and pyrite. Interfingers with Hampton Sandstone. In Gawler Craton, grades laterally and vertically into Khasta Formation. Associated with uranium mineralisation. Is overlain unconformably by Garford Formation.||||||
15170|Pidinga Formation|65260|6|Mentioned|p26, p27 Fig.20|Middle Eocene|Middle Eocene|Of Eundynie Group. Lefroy Palaeochannel. Quartz sands, clay and lignite.||||||
15170|Pidinga Formation|65385|4|Described|pS127, pS129 Fig.3, Table 1|Late Eocene|Middle Eocene|Basal unit in the Garford paleovalley. Unconformably overlies Archean-Proterozoic  basement. Unconformably overlain by Garford Formation. Gravel, carbonaceous fine to coarse sand, silt, lignite.Terrestrial to estuarine-marine conditions.||||||26-MAR-13
15170|Pidinga Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Age shown as Bartonian to Priabonian.||||||
15170|Pidinga Formation|65922|5|Briefly described|p24, p25 Tb. 4, p45 Fig.10|Late Eocene|Middle Eocene|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Underlies Garford Formation conformably. Overlies weathered basement. Mainly restricted to Narlaby Palaeochannel.||||||
15170|Pidinga Formation|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Age from Fig.2 - stratigraphic correlation chart.||||||
15170|Pidinga Formation|67462|5|Briefly described|Map legend.|Eocene|Eocene|Eucla Basin.|||Includes Maralinga and Anthony Members.|||
15170|Pidinga Formation|68128|5|Briefly described|p43, p71|Pliocene|Eocene|Gawler Craton.|||||Siltstone, carbonaceous; lignite; sand, carbonaceous. Palaeochannel fill.|01-FEB-23
15170|Pidinga Formation|68131|6|Mentioned|p71|Pleistocene|Pliocene|Flinders Island, Nuyts Domain, Gawler Craton.||||||
15170|Pidinga Formation|68715|6|Mentioned|p30 Fig.5|Bartonian|Lutetian|NW Gawler Craton, Eucla Basin.|||Anthony, Maralinga Members.|||07-APR-17
15170|Pidinga Formation|69004|4|Described|iii,  p19, p28, p32, p34, p38, p41, p115|Late Eocene|Middle Eocene|Eucla Basin. Sediments commonly form the basal infill sequence of many palaeovalleys in the Gawler-Eucla region. Informally divided into a "lower" and "upper" part on p34. Hosts groundwater aquifer in the Iluka Palaeovalley.||||Unconformably overlain by the Garford Formation. Overlain by the Khasta Formation and Narlaby Formation.|Variably oxidised carbonaceous sediments, fluvial sands and basal gravels.|
15170|Pidinga Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Ypresian|Thanetian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in shallow marine or shoreface environments. Good reservoir properties. See also p39 fig 2.14, p58, p60, p64.||||Unconformably overlies the Platypus Formation. Overlain by the Nullarbor Limestone and Wilsons Bluff Formation.|Sandstone and siltstone.|
15170|Pidinga Formation|69598|6|Mentioned|p9|Late Eocene|Middle Eocene||||Includes the Maralinga and Anthony Members.|Overlain by the Khasta Formation.||
15170|Pidinga Formation|69648|4|Described|p4,p21-22,p24,p27-28,p36,p38, map legend|Eocene|Eocene|King (1950, 1951) described sediments (Ifould Lake region) as the 'lignitic series' (occur in floor of some playa lakes), and overlying and outcropping 'lacustrine' clays and sands. Defined by Harris (1966). Harris (1966; see lithological log of Anderson, 1950) defined Formation on basis of SADME P5 drill hole at Ifould Lake on BARTON, adjacent to OOLDEA. Age: Middle to Late Eocene. Potential for placer gold deposits and other commodities. Thickness is variable: few to >50 m. This unit marks Tertiary base along most palaeochannels to NE, and within part of Eucla Basin. On OOLDEA: it unconformably overlies Cretaceous sediments of Bight Basin; toward Eucla Basin margin, it also overlies more indurated sediments of Officer Basin and crystalline basement of Gawler Craton in SE corner. Explored for coal, found lignites.||Burdunga Subgroup||Conformably overlain by/interfingers with Paling Member (Wilson Bluff Limestone); overlain by Ooldea Sand, Hampton Sandstone(conformably), Nullarbor Limestone, Garford Formation (unconformably).|Carbonaceous palaeochannel sediments (mud, sand and minor conglomerate); lignitic, and lacustrine clays and sands.|
15170|Pidinga Formation|69649|5|Briefly described|p31, p48|Eocene|Eocene|Harris (1966). Eucla Basin. Appears confined to topographic lows such as paleodrainage networks. c.80m thick. Sediment sourced fom Hiltaba Suite and Gawler Range Volcanics. Associated with uranium exploration.|||||Carbonaceous clay, silt and sand, with poor quality lignite.|
15170|Pidinga Formation|70067|5|Briefly described|Ceduna: Fig.2; p1. Regional: Fig.2|Ypresian|Thanetian|Bight Basin. Contains good quality sandstone reservoirs.||||Overlies Potoroo Formation.||
15170|Pidinga Formation|70772|6|Mentioned|p31, p41|||||||||
15170|Pidinga Formation|70778|5|Briefly described|p4|||Intersected in Nundroo 3 DDH.|||||Lignite; medium-coarse grained sand.|
15170|Pidinga Formation|71317|5|Briefly described|p143|Eocene|Eocene|||||Overlain by the Garford Formation.||
15170|Pidinga Formation|71789|6|Mentioned|p100|||||||||
15170|Pidinga Formation|71891|5|Briefly described|p6-p7, p30, p32-p40, p44-p52, p54-p55|Cenozoic|Cenozoic|Eucla Basin, Coompana Province. 30-60m thick. Interpreted to have been deposited in paleochannels and broader depressions.||||Unconformably overlies the Madura Formation. Overlain by the Hampton Sandstone.|Carbonaceous, terriginous clastic sedimentary rocks.|
15170|Pidinga Formation|72344|5|Briefly described|p4, p16,  p49, p61|||Eucla Basin. 30-60m thick package of carbonaceous terrigenous clastic sedimentary rocks deposited in topographically low settings. See also p84, p96, p160, p169.||||Overlain by the Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sands and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly carbonaceous coarse sands.|
15170|Pidinga Formation|72465|5|Briefly described|p9, 17|Tertiary|Tertiary|Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Is overlain by Hampton Sandstone.|Carbonaceous, terrigenous clastic sedimentary rocks: interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72466|5|Briefly described|p9, 17|Tertiary|Tertiary|Benbow et al. (1995). Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Overlies Madura Formation. Is overlain by Wilson Bluff Limestone and Hampton Sandstone.|Interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72467|5|Briefly described|p9, 17|Tertiary|Tertiary|Lowest unit in the Eucla Basin, Coompana Province. 30-60m thick.||||Is overlain by Hampton Sandstone.|Carbonaceous, terrigenous clastic sedimentary rocks: interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carbonaceous) coarse sands.|
15170|Pidinga Formation|72468|5|Briefly described|p9, p17|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72469|5|Briefly described|p9, p17|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72470|5|Briefly described|p9, p18|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72471|5|Briefly described|p9|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|72472|5|Briefly described|p9|||Eucla Basin. 30-60 m thick.||||Overlain by Hampton Sandstone.|Interbedded, well-sorted, fine to coarse-grained carbonaceous sand and silt with minor lignite. Flood zone clays and lignite, fluvial/estuarine channel sands, gravelly (carboneous) coarse sands.|
15170|Pidinga Formation|73099|5|Briefly described|Map legend.|Eocene|Eocene|Meramangye and Tallaringa Palaeochannels.||Burdunga Subgroup.||Overlies Bulldog Shale (Marree Subgroup). Is overlain by Garford Formation.|Green-grey, fine-grained quartz sandstone to grit, siltstone and claystone, carbonaceous in part; silcrete layers.|
15170|Pidinga Formation|73232|5|Briefly described|p8, p10, p18|Eocene|Eocene|Fluvial palaeovalley infill. Well known from palaeovalleys along the Eucla Basin northern margin. Tentatively correlated with the basal sandy unit of the Lindsay East Palaeovalley that has a thickness of 23 m in drillhole DH1a.|||||May include highly weathered, poorly to moderately sorted, coarse-grained, quartz-rich, kaolinitic sandstones that grade upward into consolidated, massive, more mature, moderately to well sorted, fine-grained, quartz-rich sandstones.|
15170|Pidinga Formation|73641|5|Briefly described|p4-5|||Basal unit in the Eucla Basin. 30-60m thick. Deposition in a palaeochannel and broader depression environment.||||Is overlain by Hampton Sandstone.|Interbedded, well-sorted, fine- to coarse-grained carbonaceous sand and silt; minor lignite, clays, channel sands, and gravelly coarse sands.|
15189|Pilbara Supergroup|22717|6|Mentioned|P19||Archean|Age of unit is 3550 to 3500 Ma||||||07-NOV-08
15189|Pilbara Supergroup|22727|6|Mentioned|p635||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|23206|5|Briefly described|p1256||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|23244|5|Briefly described|p13|||||||||
15189|Pilbara Supergroup|23325|5|Briefly described|map legend|Precambrian|Precambrian|?Pilbara Craton.||||||
15189|Pilbara Supergroup|23415|5|Briefly described|Map Legend|Archean|Archean|Includes Gorge Creek and De Grey Groups. Geological province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|23416|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|23484|5|Briefly described|p5|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|23575|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|23583|5|Briefly described|Map Legend|Archean|Archean|Geological Province Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|23585|5|Briefly described|p5|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|23598|5|Briefly described|p3|||||||||
15189|Pilbara Supergroup|23743|5|Briefly described|p1|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|23745|5|Briefly described|p6 Fig 4|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
15189|Pilbara Supergroup|23755|6|Mentioned|p2|||Geological Province: Pilbara Craton||||||
15189|Pilbara Supergroup|23783|5|Briefly described|p41|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|23793|6|Mentioned|p9|||||||||
15189|Pilbara Supergroup|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|23807|5|Briefly described|p109|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|23813|6|Mentioned|p89|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|24023|4|Described|p8|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24025|4|Described|p6|Archean|Archean|Geological Province: Pilbara Craton.  See also p8 Tb. 1.||||||07-NOV-08
15189|Pilbara Supergroup|24095|5|Briefly described|p46|||Geological Province: Pilbara Block.||||||
15189|Pilbara Supergroup|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24166|6|Mentioned|p1|||Geological Province: Pilbara Craton||||||
15189|Pilbara Supergroup|24184|5|Briefly described|p697|Archean|Archean|Geological Province: Pilbara Craton. Age: 3.51-2.94Ga||||||07-NOV-08
15189|Pilbara Supergroup|24194|5|Briefly described|p905|Archean|Archean|Age: 3.6-3.0 Ga (Pb isotope). Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24327|5|Briefly described|Map Legend|Archean|Archean|Includes the Gorge Creek, De Grey, Connterunah and Warrawoona Groups.  Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24349|5|Briefly described|Map legend|Archean|Archean|Age: c.3475-<2990Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24352|5|Briefly described|Map legend|Archean|Archean|Age: c.2925Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|24353|5|Briefly described|p1|Archean|Archean|Contains the Fortescue and Whundo Groups. Composed of Archaean greenstones and granitoids. Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|24532|5|Briefly described|Map legend|Archean|Archean|Age: c.3434-2927Ma.||||||07-NOV-08
15189|Pilbara Supergroup|24533|5|Briefly described|p4 Table 1|Archean|Archean|Greenstone sequences. Age: <3515->2945Ma.||||||07-NOV-08
15189|Pilbara Supergroup|24541|5|Briefly described|p15|Archean|Archean|Geological Province: West Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
15189|Pilbara Supergroup|24543|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|24554|6|Mentioned|p1|||Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|24590|5|Briefly described|p38|||Supracrustal sequence which constitutes the Pilbara greenstone belts, traditionally described as "layer cake stratigraphy".||||||07-FEB-11
15189|Pilbara Supergroup|38498|4|Described|p60|||||||||
15189|Pilbara Supergroup|38510|5|Briefly described|p187|||||||||
15189|Pilbara Supergroup|38544|6|Mentioned|p298|||||||||
15189|Pilbara Supergroup|38946|6|Mentioned|p361|||||||||
15189|Pilbara Supergroup|39328|6|Mentioned|Fig.3|||||||||
15189|Pilbara Supergroup|39672|6|Mentioned|Fig.2|||||||||
15189|Pilbara Supergroup|39697|2|Defined|p87|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|39837|6|Mentioned|Table 1|||||||||
15189|Pilbara Supergroup|40369|6|Mentioned|p5|||||||||
15189|Pilbara Supergroup|40596|6|Mentioned|Fig.1|||||||||
15189|Pilbara Supergroup|40933|6|Mentioned|p1|||||||||
15189|Pilbara Supergroup|41028|5|Briefly described|p227|||||||||
15189|Pilbara Supergroup|41250|5|Briefly described|p29|||||||||
15189|Pilbara Supergroup|41349|6|Mentioned|p1|||||||||
15189|Pilbara Supergroup|41353|4|Described|p68|||||||||
15189|Pilbara Supergroup|41357|6|Mentioned|p125|||||||||
15189|Pilbara Supergroup|41624|6|Mentioned|p43|||||||||
15189|Pilbara Supergroup|41767|5|Briefly described|p44|||||||||
15189|Pilbara Supergroup|41768|6|Mentioned|p9|||||||||
15189|Pilbara Supergroup|41843|6|Mentioned|Fig.1|||||||||
15189|Pilbara Supergroup|41938|6|Mentioned|p9|||||||||
15189|Pilbara Supergroup|42260|5|Briefly described|p6|||||||||
15189|Pilbara Supergroup|42661|5|Briefly described|p34|||||||||
15189|Pilbara Supergroup|43595|5|Briefly described|p73,211||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|43698|6|Mentioned|p5|||||||||
15189|Pilbara Supergroup|43779|5|Briefly described|p5||Archean|Deposited 3600-2800 Ma||||||07-NOV-08
15189|Pilbara Supergroup|43821|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|43822|5|Briefly described|map legend|Archean|Archean|Layered mafic intrusions approx. 2925 Ma.||||||07-NOV-08
15189|Pilbara Supergroup|44150|6|Mentioned|p128ff, p151, p157||||||Warrawoona, Gorge Creek, Whim Creek Groups; Louden and Negri Volcanics.|||
15189|Pilbara Supergroup|44151|6|Mentioned|p162||||||Includes Gorge Creek Group.|||
15189|Pilbara Supergroup|44152|6|Mentioned|p166, p170|||Clasts up to 5 m across, from this unit, occur in conglomerates 2500 m above the base of the Fortescue Group, suggesting either substantial paleotopography or para-depositional faulting.||||||
15189|Pilbara Supergroup|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|44229|5|Briefly described|Map Legend|Archean|Archean|Includes the De Grey, Gorge Creek and Warrawoona Groups.||||||07-NOV-08
15189|Pilbara Supergroup|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
15189|Pilbara Supergroup|46319|4|Described|p5|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|50146|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|50189|6|Mentioned|p7|Archean|Archean|||||||07-NOV-08
15189|Pilbara Supergroup|50287|5|Briefly described|Map Legend|Archean|Archean|Geological Province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|50300|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton. Includes: De Grey Group.||||||07-NOV-08
15189|Pilbara Supergroup|50302|5|Briefly described|Map Legend|Archean|Archean|Includes: Warrawoona Group, Gorge Creek Group, De Grey Group, Bookingarra Group. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|50370|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|50379|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|50381|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|50383|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
15189|Pilbara Supergroup|50427|5|Briefly described|p182 Fig.5|Archean|Archean|Age: 3520-2940 Ma. Thickness: up to 23km.||||||07-NOV-08
15189|Pilbara Supergroup|50430|5|Briefly described|p154||Archean|Greenstones - metamorphosed sedimentary and volcanic rocks, and their hypabyssal equivalents.||||||07-NOV-08
15189|Pilbara Supergroup|50544|4|Described|p18|Archean|Archean|Comprises the Coonterunah, Warrawoona, Sulphur Springs, Gorge Creek and De Grey Groups. Unconformably overlain by the Mount Bruce Supergroup.||||||07-NOV-08
15189|Pilbara Supergroup|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Warrawoona Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|60112|5|Briefly described|p106, p108, p110-112, p117,  |||A single stratigraphic sequence of Hickman (1983) grouping the older granite-greenstone rocks of the Pilbara Inlier. Deformation described.|3650 - 2850 Ma.||Includes Gorge Creek Group.|Unconformably overlain by the Fortescue Group.|Mostly metasedimentary rocks with BIF.|
15189|Pilbara Supergroup|60429|6|Mentioned|p2|Archean|Archean|||||||07-FEB-11
15189|Pilbara Supergroup|61253|4|Described|p51, p52 Fig. 2|Archean|Archean|In revised stratigraphy this group now comprises four groups: Warrawoona, Sulphur Springs, Gorge Creek and Kelly Groups. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|61264|5|Briefly described|p64 Fig. 2|||Includes Warrawoona and Kelly Groups, and Copper Gorge Formation. Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||17-MAY-06
15189|Pilbara Supergroup|61579|5|Briefly described|p58, p59|||Comprises: Coonerunah, Warrawoona, Sulphur Springs, Gorge Creek and De Grey Groups. Age: 3.51-2.94Ga. Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|63245|5|Briefly described|p4|Archean|Archean|Comprises 4 autochthonous groups, the oldest being Warrawoona Group, and Sulphur Springs, Gorge Creek and Kelly Groups. Age: 3.51-3.0Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|63367|6|Mentioned|p241-242.|||Mentioned in the context of normalisation of weathering products for REE patterns.||||||
15189|Pilbara Supergroup|63372|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|63417|5|Briefly described|Map legend|Archean|Archean|Includes the Warrawoona, Kelly and Sulphur Springs Groups.  Age range: c.3465 to ~3310Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|63420|5|Briefly described|Map legend|Archean|Archean|Includes Warrawoona, Kelly and Sulphur Springs Groups. Geological Province: Pilbara Craton.||||||07-NOV-08
15189|Pilbara Supergroup|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Comprises Soanesville, Sulphur Springs, Kelly and Warrawoona Groups. Age: from ~3525 to 3165Ma. In the east Pilbara Terrane.||||||07-FEB-11
15189|Pilbara Supergroup|63538|5|Briefly described|p2 Fig. 1, p11, p35|Archean|Archean|Includes Soanesville, Sulphur Springs, Kelly and Warrawoona Groups. Geological Province: Pilbara Craton.||||||07-FEB-11
15189|Pilbara Supergroup|63649|5|Briefly described|p200|Archean|Archean|Includes the Warrawoona, Kelly, Sulphur Springs and Gorge Creek Groups. Age: 3.51 - 3.0Ga. Thickness: ~35km. Volcanosedimentary rocks. Geological Province: Pilbara Craton / East Pilbara Terrane.||||||07-FEB-11
15189|Pilbara Supergroup|63854|5|Briefly described|p229 Fig.2, p230|||Hickman (1983). Includes the older granite-greenstone belts of the North Pilbara Craton.|||Includes the Copper Gorge Formation, the Kelly Group and the Warrawoona Group.|||
15189|Pilbara Supergroup|64326|5|Briefly described|p71 Fig. 1|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup). Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
15189|Pilbara Supergroup|64384|5|Briefly described|p22|Archean|Archean|In contact with the Shaw Batholith along its margins.||||||07-FEB-11
15189|Pilbara Supergroup|64405|5|Briefly described|p1, p20-21|Archean|Archean|Comprises Strelley Pool Fm, Warrawoona, Kelly, Sulphur Springs and Soanesville Gps. A break in the volcanic activity of the predominantly volcanic Pilbara Supergroup, allowed for the deposition of the Strelley Pool Fm units.||||||07-FEB-11
15189|Pilbara Supergroup|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Komatiitic basalt and olivine basalt; Dacite; Tremolite-chlorite-talc schist; Gabbro sills and dykes; Ultramafic volcanic rocks; Minor chert;  All metamorphosed; Interleaved amphibolite and talc-tremolite-serpentine-chlorite schist.||||||09-DEC-08
15189|Pilbara Supergroup|64621|5|Briefly described|Map legend|Archean|Archean|Includes Kelly, Salgash and Warrawoona Groups.||||||07-NOV-08
15189|Pilbara Supergroup|64632|5|Briefly described|p200, p202, p204, p205|Mesoarchean|Paleoarchean|East Pilbara Terrane. Maximum primary vertical thickness likely to have been less than 15km.|3530-3165 Ma||Soanesville Group, Sulphur Springs Group, Kelly Group, Warrawoona Group.|||
15189|Pilbara Supergroup|64653|5|Briefly described|Map Legend|Archaean|Archaean|Includes Warrawoona Group, Gorge Creek Group, De Grey Group, Budjun Creek Formation and Copper Gorge Formation. Geological Province: Pilbara Craton.||||||07-FEB-11
15189|Pilbara Supergroup|64654|5|Briefly described|Map Legend|Archaean|Archaean|Age: 3350-3335Ma. Geological Province: Pilbara Craton. Includes Kelly Group.||||||
15189|Pilbara Supergroup|64656|5|Briefly described|Map Legend|Archaean|Archaean|Includes Nullagine Group. Geological Province: Pilbara Craton.||||||26-NOV-08
15189|Pilbara Supergroup|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Warrawoona, Kelly and Gorge Creek Groups. Geological Province: Pilbara Craton.||||||
15189|Pilbara Supergroup|64747|5|Briefly described|p95, p96||||||Includes Warrawoona Group.|||
15189|Pilbara Supergroup|64936|5|Briefly described|map legend|Archean|Archean|Includes De Grey Group, Gorge Creek Group, and Warrawoona Group. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
15189|Pilbara Supergroup|65008|5|Briefly described|p2, p5, p7, p8 Fig.5, p14, p16, p41|Archean|Archean||||Includes Warrawoona Group, De Grey Group, Gorge Creek Formation, Copper Gorge Formation, and Budjan Creek Formation.|Unconformably overlain by the Mount Bruce Supergroup.||
15189|Pilbara Supergroup|65415|6|Mentioned|p118, p120 Fig.2.|Archean|Archean||||Includes Warrawoona, Gorge Creek, De Grey and Whim Creek Groups; Wyman Formation; Louden and Mount Negri Volcanics.|||
15189|Pilbara Supergroup|65724|5|Briefly described|map legend|Paleoarchaean|Paleoarchaean|Includes Kelly Group. Geol. Prov: East Pilbara Granite-Greenstone Terrane.||||||
15189|Pilbara Supergroup|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|||Includes Gorge Creek Group, Budjan Creek Formation and Warrawoona Group.|||
15189|Pilbara Supergroup|65727|5|Briefly described|Map legend|Mesoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Warrawoona, Kelly and Sulphur Springs Groups. PROBABLE MAP LEGEND ERROR > includes Dalton Suite.|||22-MAR-13
15189|Pilbara Supergroup|65825|4|Described|p5, p7 Fig.4. |Archean|Archean|Northern Pilbara Craton. Greenstones, assigned to this unit by Hickman (1983), were deposited between 3.52 and c.2.94 Ga. Van Kranendonk et al. (2004) revised this unit's stratigraphy; the changes, and correlations with the GSWA database, are detailed in Appendix 2 of the report.|||Included (Van Kranendonk et al. 2002) Coonterunah, Warrawoona, Sulphur Springs, Gorge Creek and De Grey Groups; Wyman and Golden Cockatoo Formations.||Includes multiply deformed and metamorphosed greenstones dominated by basalt, chert, banded iron-formation, ultramafic rocks, with locally abundant felsic and sedimentary rock.|
15189|Pilbara Supergroup|65827|3|Fully described|p2, p5, p6 Tb.1, p8|Mesoarchean|Paleoarchean|>3.46-3.02 Ga; formerly included Gorge Creek Group. Includes Kelly, Warrawoona and Sulphur Springs Groups. Formerly included Nimingarra Iron Formation. Unconformably underlies De Grey Supergroup, Fortescue Group. A basaltic volcanic succession.||||||
15189|Pilbara Supergroup|65828|6|Mentioned|Map legend|Archean|Archean|Pilbara Craton.|||Includes Warrawoona and De Grey Groups.|||
15189|Pilbara Supergroup|65829|6|Mentioned|p1, p7 Fig.3. |||Forms synformal greenstone belts separating broad granitic domes.||||||
15189|Pilbara Supergroup|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Pilbara Craton. Includes Warrawoona, Kelly and Sulphur Springs Groups, Strelley Pool Formation, as well as some mapped but unassigned metamorphosed ultramafic and siliciclastic rocks. Age shown as ranging from >3515 Ma to <3228 Ma.||||||09-APR-13
15189|Pilbara Supergroup|66118|5|Briefly described|p146 Fig.1, p147, 152-p153 Fig.7|||Pilbara Craton. East Pilbara Terrane. Generally well preserved and is demonstrably autochthounous. No structural repition has been observed in the EPT.|3530-3170 Ma (Van Kranendonk et al, 2006; 2007a,b)||Soanesville Group, Sulphur Springs Group, Kelly Group, Warrawoona Group||Volcanic and sedimentary rocks including basalts.|26-MAY-20
15189|Pilbara Supergroup|66122|5|Briefly described|p74|Archean|Archean|East Pilbara Terrane, Pilbara Craton.|3.53 - 3.165 Ga.||Warrawoona, Kelly, Sulphur Springs, Soanesville Groups; Strelley Pool Formation.|Is overlain unconformably by Gorge Creek Group (De Grey Supergroup).|Volcano-sedimentary rocks.|
15189|Pilbara Supergroup|66217|4|Described|p1, p2, p5, pp8-10, pp12-31.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Metavolcanic, dominantly basaltic, and metasedimentary rocks. Hickman (1983) divided this into the Warrawoona, Gorge Creek and Whim Creek Groups.|3520-3230 Ma.||Includes Warrawoona, Sulphur Springs and Kelly Groups, and Strelley Pool Formation.|Is intruded by Callina, Tambina, Emu Pool and Cleland Supersuites. Is overlain unconformably by De Grey Supergroup, Fortescue and Soanesville Groups.|Greenstone successions.|
15189|Pilbara Supergroup|66664|6|Mentioned|p3.  |||East Pilbara Terrane|||Includes Warrawoona Group as well as Strelley Pool Formation, Kelly and Sulphur Springs Groups.|||
15189|Pilbara Supergroup|66745|5|Briefly described|pp50-59.|Paleoarchean|Paleoarchean|Comprises the greenstone succession of the Paleoarchean East Pilbara Terrane. The author formally excludes the Soanesville Group from this Supergroup.|||Includes Sulphur Springs, Kelly and Warrawoona Groups and Strelley Pool Formation.|||
15189|Pilbara Supergroup|67130|6|Mentioned|p1, p13, p53|Mesoarchean|Paleoarchean|Pilbara Craton. East Pilbara Terrane. Maximum preserved thickness of 22km. Upward younging succession.|||Includes Sulphur Springs Group, Warrawoona Group, Strelley Pool Formation, Kelly Group|Unconformably overlain by De Grey Supergroup|Greenstones and granitic rocks.|
15189|Pilbara Supergroup|67197|4|Described|p1-5, p7, p9, p14, p19, p22, p29, p33-34|Paleoarchean|Paleoarchean|See also p36. Van Kranendonk et al. (2001). East Pilbara Terrane, Pilbara Craton. Now preserved in twenty greenstone belts as a carapace over almost contemporaneous (3500-3225 Ma) granitic bodies.|3525-3235 Ma.||Warrawoona, Kelly, Sulphur Springs Groups; Strelley Pool Formation.|Is overlain by Soanesville Group.|Volcanogenic and sedimentary rocks.|
15189|Pilbara Supergroup|67201|4|Described|p3, p5, p8, p10, p12 Tb.1, p20-21, p24|||In northwestern Pilbara Craton, East Pilbara Terrane. A history of at least eight successive ultramafic-mafic-felsic cyclic volcanism events, collectively 15-20 km thick. Each volcanic cycle lasted ~10-15 million years, resulting from heating events in mantle and lower crust. 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. Second break in volcanism (3315-3270 Ma) where granitic intrusion, diapiric doming, greenschist-amphibolite facies metamorphism and erosion resulted in second regional unconformity, overlain by conglomerate, sandstone, and volcaniclastic rocks at base of 3270-3235 Ma Sulphur Springs Group. Upper part of Sulphur Springs Group (komatiite and komatiitic basalt, overlain by basalt, andesite, dacite, rhyolite, and chert) interpreted as final mantle plume event of Pilbara Supergroup.|3525-3235 Ma||Sulphur Springs Group, Kelly Group, Strelley Pool Formation, Warrawoona Group|Is overlain by Gorge Creek Group, with angular unconformity.||
15189|Pilbara Supergroup|67269|6|Mentioned|p1-2, p6 Fig.3, p13|Paleoarchean|Paleoarchean|East Pilbara Terrane. Generally 15-20 km thick. Consists of three volcanic Groups and one sedimentary Formation.||||||
15189|Pilbara Supergroup|67270|5|Briefly described|p2-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.|||Warrawoona, Kelly, Sulphur Springs Groups; Strelley Pool Formation.|||
15189|Pilbara Supergroup|67668|5|Briefly described|p. 153-4; Fig.1;||Paleoarchean|Subdivided into four stratigraphic groups. Possible evidence of early life for seven formations of differing lithology is reviewed. Evidence for life includes stromatolites, microfossils, trace fossils, biominerals and isotopic signatures.|||Warrawoona, Kelly, Sulphur Springs and Soanesville Groups.|Overlain unconformably by the De Grey Supergroup (Gorge Creek Group)||
15189|Pilbara Supergroup|67888|6|Mentioned|p50|||||||||
15189|Pilbara Supergroup|68035|4|Described|p287, 293, 284|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Predominantly volcanic and 15 - 20 km thick. Thick partial sections are recognized in almost all greenstone belts of the terrane, except in the NW. Where best preserved, composed of eight ultramafic-mafic-felsic volcanic cycles. Stromatolites, microbial mats, and microfossils identified within thin sedimentary units that separate volcanic cycles.|~3530 - 3230 Ma||Includes Warrawoona, Kelly, and Sulphur Springs Groups.|||
15189|Pilbara Supergroup|68280|6|Mentioned|p1, p4||||3530-3230 Ma|||||17-JAN-23
15189|Pilbara Supergroup|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Sulphur Springs Group, Kelly Group, Warrawoona Group, Strelley Pool Formation.|||23-SEP-13
15189|Pilbara Supergroup|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|>3220 Ma||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation, Warrawoona Group.|||
15189|Pilbara Supergroup|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.|||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation, Warrawoona Group.|||23-SEP-13
15189|Pilbara Supergroup|68284|5|Briefly described|p2, 5, 7,  9|Paleoarchean|Paleoarchean|Represents the entire succession of the East Pilbara Terrane. 15-20km thick.|||Warrawoona, Kelly, Sulphur Springs Groups.||Granitic rocks.|
15189|Pilbara Supergroup|69012|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane.|||Includes the Warrawoona Group, Strelley Pool Formation, and Kelly Group.|||
15189|Pilbara Supergroup|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation, and Warrawoona Group.|||30-APR-14
15189|Pilbara Supergroup|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation, and Warrawoona Group.|||
15189|Pilbara Supergroup|69167|4|Described|geologyp_lut.csv|Mesoarchean|Paleoarchean||||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation, Warrawoona Group||Quartz--sericite schist, amphibolite; metamorphosed mafic volcanic and intrusive rocks. Amphibolites interlayered with meta-ultramafics and meta siliciclastics. Metagabbro, serpentinized metaperidotite and peridotite. Schist and metakomatiite.|
15189|Pilbara Supergroup|69185|4|Described|GEOL_LUT_CSV files|Mesoarchean|Paleoarchean|Geological Province: Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Kelly Group, Sulphur Springs Group, Warrawoona Group.||Gabbro sills and dykes; metamorphosed|
15189|Pilbara Supergroup|69299|5|Briefly described|p4, p11|||No stratigraphic subdivision of units in map legend. Geol. Prov: Pilbara Craton.|||Includes Whundo Group, De Grey Group.|||
15189|Pilbara Supergroup|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane, Whim Creek greenstone belt|||Sherlock Intrusion, Gorge Creek Group, Whundo Group, Bookingarra Group, Whim Creek Group, De Grey Group, Millindinna Intrusion, Opaline Well Intrusion|||
15189|Pilbara Supergroup|69301|4|Described|p1, p3-8, p9 Tb.1, p10-14, p20, p22|||Pilbara Craton. East Pilbara Terrane. Thickness: 15-20 km, at least eight successive major events of ultramafic-mafic-felsic cyclic volcanism. Is divided into three lithostratigraphic groups separated by two regional erosional unconformities with ages of ca 3.43 Ga and ca 3.27 Ga. Oldest zircon recorded was 3.72 Ga (Thorpe et al. 1992). Pilbara Supergroup successions includes four thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Duffer Formation and Callina Supersuite; Panorama Formation and Tambina Supersuite; Wyman Formation and Emu Pool Supersuite; Kangaroo Caves and Cleland Supersuite. In many cases, individual intrusions of supersuites are connected to overlying felsic volcanics by granitic veins, dykes, stocks, or cupolas. Stratigraphic base is not preserved due to intrusion.|3.53-3.23 Ga||Sulphur Springs Group, Kelly Group, Strelley Pool Formation, Warrawoona Group|Unconformably overlain by Budjan Creek Formation in southeast Kelly greenstone belt. Is unconformably (angular) overlain by Gorge Creek Group.||
15189|Pilbara Supergroup|69548|6|Mentioned|p2|||Pilbara region.|||||Volcano-sedimentary rocks.|
15189|Pilbara Supergroup|69563|5|Briefly described|p699|||15km thick basaltic succession. Does not include thick BIF units despite periods of prolonged weathering.|3.53-3.23 Ga.|||||
15189|Pilbara Supergroup|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Paleoarchean|Geological province: East Pilbara Terrane; Karratha 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.|3515-3235 Ma (inferred)||Includes Kelly Group, Strelley Pool Formation, Sulphur Springs Group, Warrawoona Group.||Amphibolite and amphibolite schist; metamorphosed banded iron-formation; schist; interlayered metavolcanic mafic and ultramafic rocks, metamorphosed; serpentinised peridotite and serpentine-chlorite schist; quartz sandstone.|
15189|Pilbara Supergroup|69740|5|Briefly described|p651|Paleoarchean|Paleoarchean|Plume magmatism.|3.53-3.43 Ga.||Warrawoona, Kelly Groups.||Mainly basaltic pillow lava, minor felsic and ultramafic lavas, chert layers.|
15189|Pilbara Supergroup|70022|6|Mentioned|p113-116, 121|||Comprises the oldest greenstone belt successions in the East Pilbara Terrane. Includes eight volcano-sedimentary cycles. c.15km thick.|c.3.53 - 3.23 Ga.||Warrawoona, Kelly, Sulphur Springs Groups.||Cycles involving dominantly basalt and komatiite, with thinner felsic volcanic and thin sedimentary horizons (sandstone/conglomerate, chert and BIF).|
15189|Pilbara Supergroup|70507|5|Briefly described|p430|Archean|Archean|Geological province: Pilbara Craton.|||Includes Warrawoona Group.|||
15189|Pilbara Supergroup|70729|6|Mentioned|p163-164|||Geological province: East Pilbara Terrane, Pilbara Craton.|||Includes Sulphur Springs, Kelly and Warrawoona Groups.|||
15189|Pilbara Supergroup|70733|6|Mentioned|p104-106|||Pilbara Craton. 15-20 km thick.|3530-3235 Ma.||Warrawoona, Kelly, Sulphur Springs Groups.||Predominantly mafic volcanic succession comprising a series of volcanic cycles. Conglomerate and sandstone in upper parts.|
15189|Pilbara Supergroup|70775|5|Briefly described|p6, p12, p71, p99-p100|Paleoarchean|Paleoarchean|East Pilbara Terrane.|c. 3235 Ma||Includes the Strelley Pool Formation, Sulphur Springs Group, Kelly Group and Warrawoona Group.|||
15189|Pilbara Supergroup|70826|6|Mentioned|p6 tbl 2, p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|||Includes Kelly Group, Warrawoona Group, Sulphur Springs Group|||12-MAY-20
15189|Pilbara Supergroup|70834|6|Mentioned|p298|||Marble Bar greenstone belt, Pilbara Craton.||||||
15189|Pilbara Supergroup|70884|5|Briefly described|p122-p123, 125|Mesoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Cumulative thickness of about 20km; 12km thickenss is exposed within single greenstone belts.|3.53-3.18 Ga||Includes Sulphur Springs, Kelly and Warrawoona groups, and Strelley Pool Formation.|||16-AUG-19
15189|Pilbara Supergroup|71041|6|Mentioned|p45 fig 2|Mesoarchean|Paleoarchean||3190 - >3470 Ma||Includes the Sulphur Springs Group and Soanesville Group.|Intruded by the Callina, Tambina and Cleland Supersuites.||07-NOV-17
15189|Pilbara Supergroup|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||basalt, ultramafic schist, acid volcanic rock, peridotte, komatiite, pyroxenite|
15189|Pilbara Supergroup|71270|5|Briefly described|1m_geologyl12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton.|||Includes Kelly Group.|||
15189|Pilbara Supergroup|71349|6|Mentioned|p738|||Underwent rifting c.3.2 Ga and reassembly during the c.3.07 Ga Prinsep Orogeny and the c.2.9 Ga Mosquito Creek Orogeny.||||||
15189|Pilbara Supergroup|71487|5|Briefly described|p128|Archean|Archean|Geological province: East Pilbara Terrane, Pilbara Craton.||||Includes Sulphur Springs, Kelly and Warrawoona groups, and Strelley Pool Formation.||
15189|Pilbara Supergroup|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|East Pilbara Terrane; Karratha Terrane. Subdivided into two named and 6 unnamed units.||Pilbara Supergroup|Includes Strelley Pool Formation, Warrawoona Group.||Amphibolite intruded by granite veins (50%). Amphibolite; meta. mafic volcanic + intrusive rocks; locally schistose. Meta. mafic + ultramafic rocks, some intrusive; includes local schist. Ultramafic and minor mafic schists intruded by granite veins.|
15189|Pilbara Supergroup|72064|5|Briefly described|p65-66,80|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3240 Ma (youngest zircon age)||Includes Sulphur Springs Group, Kelly Group, Strelley Pool Formation and Warrawoona Group.|||
15189|Pilbara Supergroup|72251|4|Described|p51-54,65-67|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Comprises large coherent eruptive units. Komatiite units are less common, but can be up to 400m thick (e.g. Hickman et al., 1990; Smithies et al., 2007; Van Kranendonk et al., 2007; Hickman, 2012). Intruded by younger granitic bodies in the lowermosr contact. Upperpart of the supergroup has been eroded, such that maximum original depositional thickness is unknown.|3.53-3.23 Ga||Includes Sulphur Springs, Kelly and Warrawonna groups.||Tholeiitic and komatiitic basalts interlayered with thin sedimentary horizons and locally including thick felsic volcanic units.|
15189|Pilbara Supergroup|72668|4|Described|p3, p7-8, p10-11, p14, p19, p21-25|||East Pilbara Terrane. Generally well preserved. Constituents are demonstrably autochthonous volcano-sedimentary groups. Maximum lateral thickness is almost 30km, but maximum primary vertical thickness is estimated to be less than 15km. Constituent lithologies and geochemistries are discussed. Includes inherited zircons >3500 Ma. Two sources of basaltic rocks identified: Komatiitic and low-Ti basalts.|||Includes the Soanesville Group, Sulphur Springs Group, Kelly Group and the Warrawoona Group.|Unconformably overlain by the Gorge Creek Group and the Lalla Rookh Sandstone.||13-JAN-22
15189|Pilbara Supergroup|72758|5|Briefly described|p3, p5, p17-18 Tb.1.|Archaean|Archaean|p17 Table 1 shows Metwandy Granite as part of Pilbara Supergroup, but text p3, p5 does not support this.||||Intruded by Metawandy Granite. Unconformably underlies Fortescue Group.|Includes metmorphosed mafic volcanics; dolerite, gabbro as sills, dykes and sheeted dykes; and minor chert. Generally schistose.|
15189|Pilbara Supergroup|73160|6|Mentioned|p7|||Most common type of tholeiitic basalts are high-Ti basalts.|||||Tholeiitic basalts.|
15189|Pilbara Supergroup|73598|6|Mentioned|p1207, 1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.|||Warrawoona, Kelly, Sulphur Springs Groups.|Is overlain unconformably by De Grey Supergroup.||
15198|Pilgramunna Formation|23726|5|Briefly described|p88|Middle Miocene|Late Oligocene|Of Cape Range Group. Overlying unit Vlaming Sandstone. Underlying unit Tulki Limestone Geological Province: Carnarvon Basin.||||||
15198|Pilgramunna Formation|23815|4|Described|p303|Miocene|Miocene|Geological Province: Carnarvon Basin. Overlying unit: Exmouth Sandstone (unconformable). Underlying unit: Tulki Limestone (disconformable). Max. thickness: 30 m.||||||14-DEC-04
15198|Pilgramunna Formation|24059|5|Briefly described|p138|||Geological Province: Carnarvon Basin.||||||
15198|Pilgramunna Formation|24351|5|Briefly described|Plate 4 (in pocket)|Middle Miocene|Middle Miocene|Geological Province: Exmouth Sub-basin (offshore).||||||13-DEC-07
15198|Pilgramunna Formation|30122|4|Described|p50|||||||||
15198|Pilgramunna Formation|32750|6|Mentioned|p311|||Stratigraphy||||||
15198|Pilgramunna Formation|33593|6|Mentioned|p107|||Refs Condon and others,2nd ed 1955||||||
15198|Pilgramunna Formation|34363|6|Mentioned|p56|||See also Fig.7. Lower Miocene.||||||
15198|Pilgramunna Formation|35105|6|Mentioned|Fig.5|||||||||
15198|Pilgramunna Formation|35282|6|Mentioned|p27|||||||||
15198|Pilgramunna Formation|36257|6|Mentioned|Table 2.1|||||||||
15198|Pilgramunna Formation|36890|3|Fully described|p303|||||||||
15198|Pilgramunna Formation|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
15198|Pilgramunna Formation|39427|4|Described|Table 1|||||||||
15198|Pilgramunna Formation|40617|6|Mentioned|p16|||Mention P18||||||
15198|Pilgramunna Formation|40800|6|Mentioned|p25|||||||||
15198|Pilgramunna Formation|41271|3|Fully described|p185|Cenozoic|Cenozoic|Of Cape Range Group.||||||19-NOV-08
15198|Pilgramunna Formation|41438|4|Described|p111|||||||||
15198|Pilgramunna Formation|42116|6|Mentioned|p69|||||||||
15198|Pilgramunna Formation|45015|5|Briefly described|map legend|Tertiary|Tertiary|Of the Yardie Group. Age is Late Tertiary. Geological Province: Carnarvon Basin.||||||31-MAY-06
15198|Pilgramunna Formation|46805|6|Mentioned|Fig.2|||||||||
15198|Pilgramunna Formation|46983|6|Mentioned|Fig.2|||||||||
15198|Pilgramunna Formation|61155|5|Briefly described|p15|Middle Miocene|Middle Miocene|Of the Cape Range Group.  Overlies and interfingers with Trealla Limestone; overlain by and interfingers with Vlaming Sandstone. Age: ~13-~10Ma. Thickness: 30m.  Geological Province: Carnarvon Basin /onshore.||||||
15198|Pilgramunna Formation|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Of the Yardie Group.||||||
15198|Pilgramunna Formation|62837|5|Briefly described|Stratigraphic columns|Late Miocene|Late Miocene|Age: >10Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
15198|Pilgramunna Formation|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef. Tertiary limestone.||||Overlies Tulki Limestone. Is overlain by Vlaming and Exmouth Sandstones.||
15198|Pilgramunna Formation|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Overlain by Vlaming Sandstone, Exmouth Sandstone, overlies Trealla Limestone|Planar cross bedded sandstone.|
15198|Pilgramunna Formation|70066|5|Briefly described|Regional: Fig.6|Serravallian|Serravallian|Exmouth Sub-basin, Northern Carnarvon Basin.||||Overlies Trealla Limestone. Is overlain by Exmouth Sandstone.||
15198|Pilgramunna Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, calcarenite|
15228|Pincombe Formation|22547|5|Briefly described|p24|Cryogenian|Stenian|Of the Carr Boyd Group.  Age: 891 +/- 149 Ma.||||||14-NOV-06
15228|Pincombe Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group.||||||23-NOV-06
15228|Pincombe Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15228|Pincombe Formation|32660|5|Briefly described|Table 6|||||||||
15228|Pincombe Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15228|Pincombe Formation|32701|6|Mentioned|p7|||||||||
15228|Pincombe Formation|32728|5|Briefly described|Table 6|||See also p47.||||||23-NOV-06
15228|Pincombe Formation|36551|6|Mentioned|Table 12|||||||||
15228|Pincombe Formation|37462|6|Mentioned|Fig.4.13|||||||||
15228|Pincombe Formation|40792|6|Mentioned|Fig.5|||||||||
15228|Pincombe Formation|41158|6|Mentioned|p19|||||||||
15228|Pincombe Formation|42175|5|Briefly described|Fig.2 P200|||||||||
15228|Pincombe Formation|44155|5|Briefly described|p250 Tb.3-10|||Up to 2500m thick.||Carr Boyd Group||Gradational contact with underlying Stonewall Sandstone.|Red and green siliceous siltstone, and fine sandstone, blocky quartz sandstone; minor micaceous shale.|
15228|Pincombe Formation|45047|6|Mentioned|Plate 17|||||||||
15228|Pincombe Formation|45112|6|Mentioned|Table 16|||||||||
15228|Pincombe Formation|48938|6|Mentioned|p76|||Equiv. Legune Fm.||||||
15228|Pincombe Formation|65417|5|Briefly described|pp156-159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Age from Bofinger (1967) recalculated by Plumb et al. (1981). Correlated with Legune Formation of the Fitzmaurice Group (NT). Braided-delta progradation and retreat.|891 +/- 149 Ma (Rb-Sr whole rock).|Topmost unit in Carr Boyd Group.||Conformably overlies Stonewall Sandstone.||
15228|Pincombe Formation|69435|5|Briefly described|p20:3|||Carr Boyd Basin. A previous correlation  with the Legune Formation (Fitzmaurice Group, NT) is called into question.||Carr Boyd Group.||Overlies Stonewall Sandstone.||12-JUL-16
15228|Pincombe Formation|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlies Stonewall Sandstone||
15228|Pincombe Formation|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Carr Boyd Group.|||Siliceous siltstone and fine-grained sandstone, micaceous shale, quartz sandstone|
15231|Pindilya Formation|12729|6|Mentioned|Fig. 6|Miocene|Miocene|||||Adjacent to the Trealla Limestone.|Sandstone.|
15231|Pindilya Formation|14228|6|Mentioned|p5 fig 2, p9|Miocene|Miocene|Merlinleigh Sub-basin.||||||
15231|Pindilya Formation|23572|5|Briefly described|p8 Fig. 6|Miocene|Miocene|Geological Province: Carnarvon Basin.||||||
15231|Pindilya Formation|23726|5|Briefly described|p88|Middle Miocene|Oligocene|Overlying unit Peron Sandstone. Underlying unit Tulki Limestone. Geological Province: Carnarvon Basin.||||||
15231|Pindilya Formation|23815|4|Described|p299, 302|Eocene|Eocene|Geological Province: Carnarvon Basin. Max. thickness: 27 m.||||||18-APR-05
15231|Pindilya Formation|23816|4|Described|p253, 254|Eocene|Eocene|Geological Province: Perth Basin. Underlying units: Nangetty Formation and Homwood Shale (both unconformable). Max. thickness: 3 m.||||||16-DEC-04
15231|Pindilya Formation|23935|5|Briefly described|p11 Fig.7|Miocene|Miocene|Geological Province: Southern Carnarvon Basin.||||||
15231|Pindilya Formation|24059|5|Briefly described|p150|Tertiary|Tertiary|Ggeological Province: Carnarvon Basin. Maximum thickness: 27m.||||||
15231|Pindilya Formation|24114|5|Briefly described|p8|Tertiary|Tertiary|||||||
15231|Pindilya Formation|24160|6|Mentioned|p65 Fig.27.|Miocene|Miocene||||||Poorly sorted sandstone, conglomerate, and silcrete.|
15231|Pindilya Formation|31051|6|Mentioned|p.83.|||||||||
15231|Pindilya Formation|32648|6|Mentioned|p32|||Eocene||||||
15231|Pindilya Formation|32750|6|Mentioned|p310|||Equiv. Merlinleigh section||||||
15231|Pindilya Formation|33594|2|Defined|p39|Tertiary|Tertiary|||||||
15231|Pindilya Formation|35105|6|Mentioned|Fig.5|||||||||
15231|Pindilya Formation|35282|6|Mentioned|Fig.19|||||||||
15231|Pindilya Formation|36257|6|Mentioned|Table 2.1|||||||||
15231|Pindilya Formation|36293|6|Mentioned|p203|||||||||
15231|Pindilya Formation|36890|3|Fully described|p253|||See also P302.||||||
15231|Pindilya Formation|38493|4|Described|p36|||||||||
15231|Pindilya Formation|38494|4|Described|p29|||||||||
15231|Pindilya Formation|40336|5|Briefly described|p18|||||||||
15231|Pindilya Formation|40339|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15231|Pindilya Formation|40340|5|Briefly described|p15|||||||||
15231|Pindilya Formation|40341|6|Mentioned|Map legend|Miocene|Miocene|||||||
15231|Pindilya Formation|40342|6|Mentioned|Map legend|middle Miocene|middle Miocene|Prob.Middle Miocene||||||
15231|Pindilya Formation|40343|5|Briefly described|p12|||||||||
15231|Pindilya Formation|40617|6|Mentioned|p18|||||||||
15231|Pindilya Formation|41271|3|Fully described|p193|||||||||
15231|Pindilya Formation|41438|6|Mentioned|Fig.23|||||||||
15231|Pindilya Formation|42116|6|Mentioned|p69|||||||||
15231|Pindilya Formation|43255|5|Briefly described|map legend|Pleistocene|Miocene|Age ?Miocene to Pleistocene.||||||
15231|Pindilya Formation|43256|5|Briefly described|19||Tertiary|||||||
15231|Pindilya Formation|43835|5|Briefly described|Map Legend||Tertiary|||||||
15231|Pindilya Formation|44144|6|Mentioned|p520|||Deposition was by sheet-flood processes.||||||
15231|Pindilya Formation|44532|4|Described|p.9, map|||(P.F.). (G50-5).||||||
15231|Pindilya Formation|44533|5|Briefly described|map legend||Eocene|Eocene.||||||
15231|Pindilya Formation|45015|5|Briefly described|map legend|Tertiary|Tertiary|Age is Early Tertiary. Geological Province: Carnarvon Basin.||||||31-MAY-06
15231|Pindilya Formation|45016|14|Not recorded|p.69,109||Eocene|?Eocene.||||||
15231|Pindilya Formation|48823|5|Briefly described|p2, p3 Tb. 1|||See also p27-28.||||||
15231|Pindilya Formation|61155|5|Briefly described|p15|Middle Miocene|Middle Miocene|Of the Cape Range Group. Overlain by and interfingers with Trealla Limestone; overlies and interfingers with Lamont Sandstone. Thickness: 20m.  Geological Province: Carnarvon Basin /onshore.||||||
15231|Pindilya Formation|61958|5|Briefly described|Map sheet 1|Paleogene|Paleogene|||||||
15231|Pindilya Formation|66125|6|Mentioned|p132|Miocene|Oligocene|Onshore Carnarvon Basin.||||||
15231|Pindilya Formation|67200|5|Briefly described|p8 fig 6, |Miocene|Oligocene|||||Unconformably overlies Tulki Limestone, overlain by Peron Sandstone|Commonly massive pebbly sandstone and limestone with inverterbrate macrofossils.|
15231|Pindilya Formation|69028|5|Briefly described|Map Legend|Miocene|Miocene||||||Poorly sorted sandstone, commonly lithic, and granule to pebble conglomerate; generally very silicified.|17-SEP-15
15231|Pindilya Formation|69166|5|Briefly described|geologyp_lut.csv|Miocene|Miocene||||||Poorly sorted sandstone, commonly lithic, and granule to pebble conglomerate; generally very silicified|
15231|Pindilya Formation|69182|6|Mentioned|Ch3 p13|Miocene|Miocene|Merlinleigh Sub-basin, Carnarvon Basin.||||||
15231|Pindilya Formation|70795|4|Described|100k_geologyp_lut.csv|Pliocene|Miocene|Also 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|23-5 Ma||||Poorly sorted sandstone, commonly lithic, and granule to pebble conglomerate; generally very silicified.|
15231|Pindilya Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, silcrete, sandstone|
15231|Pindilya Formation|72034|5|Briefly described|500k_interpgeop16_lut|Miocene|Miocene|Southern Carnarvon Basin.|||||Poorly sorted sandstone, commonly lithic, and granule to pebble conglomerate; generally very silicified.|
15260|Pinjian Chert Breccia|22701|5|Briefly described|Fig2,p39|||Hamersley Basin. Overlies Carawine Dolomite of Hamersley Group.||||||
15260|Pinjian Chert Breccia|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlying unit Carawine Dolomite.||||||
15260|Pinjian Chert Breccia|23583|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
15260|Pinjian Chert Breccia|23585|4|Described|p19|Paleoproterozoic|Paleoproterozoic|Overlain by Manganese Subgroup. Underlain by Carawine Dolomite. Geological Province: Hamersley Basin.||||||07-NOV-08
15260|Pinjian Chert Breccia|23594|4|Described|p18|Proterozoic|Archean|Underlain by  Carawine Dolomite. Geological Province: Hamersley Basin.||||||07-NOV-08
15260|Pinjian Chert Breccia|23745|4|Described|p15|Paleoproterozoic|Paleoproterozoic|See also page 7 Fig 5.||||||07-NOV-08
15260|Pinjian Chert Breccia|23746|4|Described|p21|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15260|Pinjian Chert Breccia|24025|5|Briefly described|p14|||||||||
15260|Pinjian Chert Breccia|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Hamersley Basin||||||
15260|Pinjian Chert Breccia|29850|6|Mentioned|p1020|||||||||
15260|Pinjian Chert Breccia|30503|6|Mentioned|p10|||Also mention Table 1||||||
15260|Pinjian Chert Breccia|30881|5|Briefly described|p527|||||||||
15260|Pinjian Chert Breccia|34135|4|Described|Table 1|||Middle Proterozoic. See also Table 2 and pp7,12,14,18.||||||24-JUL-07
15260|Pinjian Chert Breccia|37460|3|Fully described|p122|||||||||
15260|Pinjian Chert Breccia|39424|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15260|Pinjian Chert Breccia|39426|4|Described|p12|||||||||
15260|Pinjian Chert Breccia|39697|4|Described|p126|||||||||
15260|Pinjian Chert Breccia|41669|3|Fully described|FD|||||||||
15260|Pinjian Chert Breccia|41768|5|Briefly described|Table 1|||See also P30||||||
15260|Pinjian Chert Breccia|42020|5|Briefly described|p316|||||||||
15260|Pinjian Chert Breccia|42352|6|Mentioned|p22||Tertiary|||||||
15260|Pinjian Chert Breccia|42704|5|Briefly described|Plate 2E|Proterozoic||Chert breccia, poorly banded chert.||||||07-AUG-08
15260|Pinjian Chert Breccia|43055|4|Described|p17, Table 4|||||||||
15260|Pinjian Chert Breccia|43056|5|Briefly described|Map Legend|||of Mount Bruce Supergroup||||||
15260|Pinjian Chert Breccia|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).||||||
15260|Pinjian Chert Breccia|44189|5|Briefly described|Map legend||Proterozoic|||||||
15260|Pinjian Chert Breccia|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
15260|Pinjian Chert Breccia|44297|14|Not recorded|p.5,7,9-10,12,15|||(F51-9).||||||
15260|Pinjian Chert Breccia|44438|14|Not recorded|map legend||Mesoproterozoic|M.Proterozoic.||||||
15260|Pinjian Chert Breccia|45923|4|Described|p.69|||On many pages - pp66,75-79,104,145, map. Age uncertain.||||||24-JUL-07
15260|Pinjian Chert Breccia|46319|6|Mentioned|p15|||Replaced by Pinjian Breccia.||||||
15260|Pinjian Chert Breccia|50287|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||
15260|Pinjian Chert Breccia|50544|4|Described|p53, p15 Tb. 1|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Carawine Dolomite; unconformably overlain by the mesas of the Paterson Formation.  Age: <2400Ma.||||||07-NOV-08
15260|Pinjian Chert Breccia|50555|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Chert breccia and poorly bedded chert.  Overlies Carawine Dolomite; underlies Paterson Formation.  Geological Province: Pilbara Craton.||||||07-NOV-08
15260|Pinjian Chert Breccia|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
15260|Pinjian Chert Breccia|61575|5|Briefly described|p759|||Overlies the Carawine Dolomite. Interpreted to be a silicified palaeokarst deposit.||||||
15260|Pinjian Chert Breccia|63139|5|Briefly described|p50|Neoarchean|Neoarchean|Overlies Carawine Dolomite; overlain by the Manganese Group. Interpreted to be a siliceous replacement deposit formed by karstic weathering of the Carawine Dolomite.||||||07-NOV-08
15260|Pinjian Chert Breccia|63417|5|Briefly described|Map legend|Paleoproterozoic||Overlies Carawine Dolomite. Chert breccia and poorly bedded chert.||||||07-NOV-08
15260|Pinjian Chert Breccia|64384|5|Briefly described|p40|||Unconformably overlies Carawine Dolomite.||||||07-FEB-11
15260|Pinjian Chert Breccia|64580|4|Described|map legend|Paleoproterozoic|Neoarchean|Chert breccia and poorly bedded chert; overlies CARAWINE DOLOMITE.||||||09-DEC-08
15260|Pinjian Chert Breccia|65724|5|Briefly described|map legend|||Overlies Carawine Dolomite. Unconformable under Paterson Formation. Chert breccia and poorly bedded chert. Age: younger than c. 2548 Ma, older than Mesoproterozoic. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
15260|Pinjian Chert Breccia|65825|4|Described|p7 Fig.4, p24, p26.|Paleoproterozoic|Neoarchean|Thought to have formed by deep weathering of Carawine Dolomite. Upper surface has polished grooved pavements below the overlying Paterson Formation. Locally capped by siliceous duricrust, thought to be derived by deep weathering and secondary silicification.  Hosts supergene manganese mineralization in the form of surface sheets and lens-shaped mounds.||Unit in Mount Bruce Supergroup.||Overlies Carawine Dolomite. Is overlain by Paterson Formation.|Consists of angular fragments of chert and layered chert in a siliceous matrix; locally rich in iron and manganese oxides giving the rock a black to dark-brown colour and semimetallic lustre.|
15260|Pinjian Chert Breccia|65827|6|Mentioned|p43|||Intruded by dykes.||||||21-JAN-22
15260|Pinjian Chert Breccia|65828|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||Overlies Carawine Dolomite.|Chert breccia, locally bedded.|
15260|Pinjian Chert Breccia|65829|3|Fully described|p1, p7 Fig.3, p25, p27, pp35-36.|Paleoproterozoic|Paleoproterozoic|Deposition concordant with weathering and karstification of Carawine Dolomite; fills fissures, caves and dolines. Weathering in Cenozoic has led to new caves and collapses. A strongly outcropping unit characterised by spinifex-covered high rounded hills. Fe and Mn oxides are derived from Carawine Dolomite. Is onlapped by Manganese Group, and like that Group, hosts manganese mineralization with a high Fe content in the Ripon Hills area and Midgengadge Creek. Evidence of Permian glaciation is preserved on the surface of this unit.|c.2500 Ma.|||Unconformably overlies Carawine Dolomite with a highly irregular contact.|Randomly mixed angular fragments of chert and banded chert; chaotically or crudely bedded; silicified and further weathered in Cenozoic; locally enriched in iron and manganese oxides.|
15260|Pinjian Chert Breccia|67183|4|Described|p639-49, p668|Paleoproterozoic|Neoarchean|In general it represents the ~Paleoproterozoic weathering product of the Carawine Dolomite formed during ca 1300 My hiatus from deposition of the dolomite to deposition of the unconformably overlying Manganese Subgroup.||Hamersley Group||Unconformably overlies the Carawine Dolomite, unconformably overlain by the Stag Arrow Formation (Manganese Subgroup) .|Mn mineralisation (ore), in situ chert breccia - angular to sub-angular fragments of bedding parallel chert bands. Chert fragments recemented in silica. Variable thickness.|
15260|Pinjian Chert Breccia|67202|4|Described|p41, p52, p54, p66, p74, p119-120, p150|Paleoproterozoic|Paleoproterozoic|See also p258, p281. Ore host. Poorly magnetised: not discriminated in aeromagnetic data. Has a silcrete duricrust. Associated with the Mn deposits of the Woodie Woodie mine. Appears as Pinjian Chert Member [?] on p74 and p150. Conductivity described and imaged.||Hamersley Group.||Unconformably overlies Carawine Dolomite. Is overlain unconformably by Woblegun and Waltha Woora Formations.|Angular chert fragments in a siliceous chert matrix.|15-FEB-18
15260|Pinjian Chert Breccia|67829|5|Briefly described|p448, p451, pp453-454.|||Very thick and complex. Silica leached from Brockman BIF is argued (Goode 2012) to have concentrated in this unit, replacing the Carawine Dolomite in part. Others argue it is either a surface silicified feature of the Carawine Dolomite, or epithermal alteration. Total volume of this unit estimated at c.100 km3 (Blake et al. 2011).||||Is overlain by Manganese Group.||
15260|Pinjian Chert Breccia|69167|4|Described|geologyp_lut.csv|Mesoproterozoic|Neoarchean|||||Overlies Carawine Dolomite|Chert breccia and poorly bedded chert;|
15260|Pinjian Chert Breccia|69185|5|Briefly described|GEOL_LUT_CSV files|Paleoproterozoic|Neoarchean|See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||||Underlain by Carawine Dolomite.|Chert breccia and poorly bedded chert.|
15260|Pinjian Chert Breccia|69563|6|Mentioned|p691 Fig.1|||||||||
15260|Pinjian Chert Breccia|69590|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Neoarchean|Events: Western Australian events. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2597-1000 Ma (inferred)||||Chert breccia and poorly bedded chert; overlies Carawine Dolomite|
15260|Pinjian Chert Breccia|70826|6|Mentioned|p8|Neoarchean|Neoarchean|Included in the lower Hamersley Group, although its age is uncertain.||Hamersley Group, lower||Overlies the Carawine and Wittenoom Dolomites.||13-MAY-20
15260|Pinjian Chert Breccia|70936|6|Mentioned|p72|Archean|Archean|Geological province: Pilbara Craton.||||||
15260|Pinjian Chert Breccia|71003|6|Mentioned|p72|Archean|Archean|Pilbara Craton. Unconformably overlain by a tuffaceous horizons which are dated.||||||
15260|Pinjian Chert Breccia|71042|4|Described|p63, p64 fig 1, p66 fig 2|Paleoproterozoic|Paleoproterozoic|Oakover Basin. Up to 100m thick in places. Hosts the Tally Ho and Contact manganese deposits where it contacts the Carawine Dolomite. See also p67-p72, p74, p76-p87, p89, p91, p96-p99.|ca 1300 Ma|||Overlies the Carawine Dolomite. Unconformably overlain by the Googenhama Formation and the Manganese Group.|Breccia of angular to subangular chert bands.|
15260|Pinjian Chert Breccia|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, sedimentary breccia|
15260|Pinjian Chert Breccia|71808|6|Mentioned|p39|||||||||
15260|Pinjian Chert Breccia|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Neoarchean|Hamersley Basin.||||Overlies Carawine Dolomite.|Chert breccia and poorly bedded chert.|
15260|Pinjian Chert Breccia|73184|6|Mentioned|p188|Paleoproterozoic|Paleoproterozoic|Pilbara Craton. Striated surfaces in the Oakover River area with overlying tillites evidence of an early Permian ice-sheet.||||||
15264|Pinkerton Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|23937|6|Mentioned|p76 App. 1|||Of the Auvergne Group.||||||02-NOV-04
15264|Pinkerton Sandstone|24122|3|Fully described|p10, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlies Saddle Creek Formation.  Approximately 30m thick.  Geological Province: Victoria Basin.||||||
15264|Pinkerton Sandstone|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Saddle Creek Formation; overlain by Lloyds Creek Formation. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group. Geological Province: Victoria Basin.||||||12-SEP-11
15264|Pinkerton Sandstone|28255|4|Described|p67, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Auvergne Group. Massive quartz sandstone. Conformably overlain by Lloyd Creek Formation; conformably overlies Saddle Creek Formation. Max. thickness100m. See also p68 Tb. 6.||||||
15264|Pinkerton Sandstone|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
15264|Pinkerton Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
15264|Pinkerton Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
15264|Pinkerton Sandstone|32660|5|Briefly described|Table 6|||||||||
15264|Pinkerton Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Massive quartz sandstone, siltstone, minor mudstone.||||||12-SEP-11
15264|Pinkerton Sandstone|32700|4|Described|Table 1|||Lithology p14. Refers Randal (1962).||||||23-NOV-06
15264|Pinkerton Sandstone|32701|4|Described|Table 1|||Adelaidean. Auvergne Group. See p9.||||||23-NOV-06
15264|Pinkerton Sandstone|32728|6|Mentioned|Fig.14|||||||||
15264|Pinkerton Sandstone|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Quartz sandstone, minor siltstone.||||||12-SEP-11
15264|Pinkerton Sandstone|33373|3|Fully described|p10|||Table 2.||||||
15264|Pinkerton Sandstone|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and medium blocky quartz sandstone. Conformable on Saddle Creek Formation. Max. thickness: ~50m.||||||28-APR-05
15264|Pinkerton Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15264|Pinkerton Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and medium quartz sandstone.||||||27-APR-05
15264|Pinkerton Sandstone|41660|5|Briefly described|Map legend|Mesoproterozoic||Of Auvergne Group. Quartz arenite, flaggy to well bedded, cross-bedded. Min thickness: up to at least 40m.||||||07-OCT-05
15264|Pinkerton Sandstone|41661|5|Briefly described|Table 1|||||||||
15264|Pinkerton Sandstone|45112|6|Mentioned|Table 6|||||||||
15264|Pinkerton Sandstone|48938|2|Defined|p43|Proterozoic|Proterozoic|Measured section p96. ?Adelaidean.||||||23-NOV-06
15264|Pinkerton Sandstone|48942|3|Fully described|p68|||||||||
15264|Pinkerton Sandstone|48943|4|Described|p76|||||||||
15264|Pinkerton Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Saddle Creek Formation. Overlain by Lloyd Creek Formation. Silica cemented quartz sandstone, minor siltstone and mudstone.||||||21-JUL-04
15264|Pinkerton Sandstone|60682|4|Described|p9 Table 2|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Saddle Creek Formation. Conformably overlain by Lloyd Creek Formation. Max. thickness: 375m. Quartz sandstone, minor siltstone and mudstone. Geological Province: Victoria Basin.||||||23-NOV-06
15264|Pinkerton Sandstone|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
15264|Pinkerton Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Silica cemented quartz sandstone, minor siltstone and mudstone||||||
15264|Pinkerton Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Saddle Creek Formation. Is overlain by Lloyd Creek Formation.||
15264|Pinkerton Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Overlies Saddle Creek Formation.|Fine and medium quartz sandstone.|
15264|Pinkerton Sandstone|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Silica cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|68733|5|Briefly described|p177 Fig.2, p179, p185, p189 Fig.8, p192|Cryogenian|Cryogenian|Victoria Basin. Sm-Nd isotope data tabulated.||Of the Auvergne Group.||||05-DEC-17
15264|Pinkerton Sandstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Saddle Creek Formation. Is overlain by Lloyd Creek Formation.||12-JUL-16
15264|Pinkerton Sandstone|69441|4|Described|p26:2-6|Neoproterozoic|Neoproterozoic|Forms a resistant capping on the main escarpments and plateaux of the Pinkerton and Yambarra Ranges. Typically 100-200m thick, up to 375m locally. Marine transgression, rare periods of brine-logging. Offset by Pinkerton Range Fault.||Auvergne Group.||Conformably overlies Saddle Creek Formation. Is overlain conformably by Lloyd Creek Formation.|Basal medium-grained silica-cemented quartz sandstone up to 30m thick; overlain by mudstone, siltstone and sandstones. Dolomitic phases present.|12-JUL-16
15264|Pinkerton Sandstone|69673|5|Briefly described|p188|||375m thick.||Auvergne Group|||Quartz sandstone, mudstone, siltstone and fine grained sandstone.|
15264|Pinkerton Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Silica cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group||Overlies Saddle Creek Formation. Is overlain by Moonlight Valley Tillite.|Fine and medium quartz sandstone.|21-JAN-22
15264|Pinkerton Sandstone|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Conformably overlies Saddle Creek Formation.|Silica-cemented quartz sandstone, minor siltstone and mudstone.|
15264|Pinkerton Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
15264|Pinkerton Sandstone|71302|4|Described|p1,6-7,58-64,72-74|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Forms a resistant cap on main escarpments and dissected plateauz on AUVERGNE 1:250 000 map sheet (Sweet et al., 1974a, b; Dunster et al., 2000), reaching up to 375m thick. Deposited in high-energy nearshore conditions with more terrigenous clastic input than underlying Saddle Creek Formation or overlying Lloyd Creek Formation (Dunster et al., 2000; Dunster and Ahmed, 2013b). Sample GA 1957134 (quartz sandstone) yielded an interpreted (weighted mean 238U/206Pb) maximum depositional age of 973+\-14 Ma. Sample description, locality, zircon description, SHRIMP analyses and results are discussed.||Unit of Auvergne Group.||Overlain by Lloyd Creek Formation. Underlain conformably by Saddle Creek Formation.|Mudstone, siltstone, fine-grained, ferruginous, feldpsathic quartz sandstone and dolomitic phases.|09-DEC-19
15264|Pinkerton Sandstone|73083|6|Mentioned|p8|||||||||
15279|Pinyinna beds|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
15279|Pinyinna beds|22647|6|Mentioned|Fig 1 on p 113|||||||||
15279|Pinyinna beds|22804|5|Briefly described|p441|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|22826|4|Described|p568|Neoproterozoic|Neoproterozoic|The Pinyinna beds are time equivalents of the Bitter Springs Formation in the southwest of the Basin.||||||
15279|Pinyinna beds|24301|4|Described|p14|Neoproterozoic|Neoproterozoic|Also referred to as Pinyinna Beds on p7 Tb.2 and p15. Lithology: siltstone and dolostone.  Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Grey to purple muscovite-quartz phyllite, thinly laminated; crenulated in places. Geological Province: Amadeus Basin.||||||16-JUN-09
15279|Pinyinna beds|24496|5|Briefly described|p21 Tb.2|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15279|Pinyinna beds|41884|6|Mentioned|p70|||||||||
15279|Pinyinna beds|42940|6|Mentioned|p 1|||||||||
15279|Pinyinna beds|45155|6|Mentioned|p47|||||||||
15279|Pinyinna beds|45170|6|Mentioned|p5|||||||||
15279|Pinyinna beds|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite.  Underlies Winnall beds, Inindia beds.||||||22-DEC-09
15279|Pinyinna beds|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies Dean Quartzite. Underlies Inindia beds, Winnall beds.||||||23-NOV-06
15279|Pinyinna beds|60572|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey, quartz-muscovite phyllite.   Geological Province: Amadeus Basin.||||||23-DEC-09
15279|Pinyinna beds|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Deformed basal sediments of Amadeus Basin.||||||22-FEB-05
15279|Pinyinna beds|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone,red, green and pale grey fissile siltstone, dolomitic siltstone.  Geological Province: Amadeus Basin.||||||11-JAN-05
15279|Pinyinna beds|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz-muscovite phyllite. Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|60683|4|Described|p25, p9 Tb. 1|Neoproterozoic|Neoproterozoic|Sequence of siltstone and dolomite - grey quartz-muscovite phyllite, crystalline dolostone.  Conformably overlie Pottoyu Granite and Dean Quartzite. Age: probably c.820Ma. Thickness: >100m. Geol. Prov: Amadeus Basin. Equiv. to Bitter Springs Formation.||||||20-APR-05
15279|Pinyinna beds|61154|5|Briefly described|p18, p5 Tb. 1|Neoproterozoic|Neoproterozoic|Grey to purple quartz-muscovite phyllite; crystalline dolostone; fine sst; red, green and pale fissile sltst; dolomitic sltst.  Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges. Typ sect.thickness:250m||||||19-JUL-05
15279|Pinyinna beds|61306|5|Briefly described|p32|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pinyinna  Geological Province: Amadeus Basin.||||||23-NOV-06
15279|Pinyinna beds|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15279|Pinyinna beds|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15279|Pinyinna beds|62989|6|Mentioned|p40|||Geological Province: Amadeus Basin.||||||07-FEB-08
15279|Pinyinna beds|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
15279|Pinyinna beds|65256|4|Described|piii, p5, p6 Tb.1, p8, p16-18, p21, p29|Cryogenian|Stenian|[Formerly Pinyinna Beds (in Forman 1966)]. Probably ~800-820 Ma. Sourced from local 1040-1080 Ma granites and volcanics. Phyllitic to schistose in character. >100m thick.||||Disconformably underlies Winnall beds, Inindia beds, Mount Currie Conglomerate; conformably overlies Dean Quartzite; correlative of the Bitter Springs Formation.|Red and grey shales, grey phyllite, crystalline brown and grey, foetid, stromatolitic dolostone.|19-MAY-14
15279|Pinyinna beds|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Dean Quartzite. Is overlain unconformably by Boord Formation.||
15279|Pinyinna beds|67856|4|Described|p341 tab 4-8, p338, 335, 337, 344, 348|Neoproterozoic|Neoproterozoic|Type section: Pinyinna Range 24o35'S, 129o51'E.  Stromatolites poorly preserved; age unknown. Misspelt as Pinnyinna beds in fig 4-30 p338.||||Overlain by Mount Currie Conglomerate (unconformably). equivalent to Bitter Springs Formation. Overlies Dean Quartzite (unconformably).|Sandstone, siltstone, limestone.|
15279|Pinyinna beds|68270|4|Described|p679,683|Tonian|Tonian|Amadeus Basin.||||Overlain unconformably by Inindia beds.||03-JUL-19
15279|Pinyinna beds|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|69436|5|Briefly described|p21:4, 17-19|Neoproterozoic|Neoproterozoic|Olia Chain, Amadeus Basin. Involved in thin- and thick-skinned deformation by the Petermann Orogeny. At the top of this unit is a decollement surface below which basement and basal Amadeus Basin rocks were structurally interleaved.||||Is structurally interleaved with Dean Quartzite.||12-JUL-16
15279|Pinyinna beds|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 1.||||Overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation.||12-JUL-16
15279|Pinyinna beds|69438|2|Defined|p23:2-4, 9-10, 14-15, 18, 44, 52|Cryogenian|Cryogenian|Forman (1966), who described it as a metamorphosed equivalent of Bitter Springs Formation. SW Amadeus Basin. Type area in the Pinyinna Range, where it is over 200m thick. Appears as Pinyinna Beds on 23:4. Part of Supersequence 1 of the Centralian A Superbasin. Metamorphosed to amphibolite-grade facies, decreasing to greenschist facies to the N. Detrital zircon age populations suggest provenance from the Musgrave Province. Maximum age from SHRIMP U-Pb analyses of detrital zircons (Close et al., 2004); minimum age from intrusive dyke. Hosts uneconomic base metal occurrences.|Between 1058 +/- 31 Ma and c.820 Ma.|||Conformably (gradationally) overlies Dean Quartzite. Lateral equivalent of Bitter Springs Formation. Is intruded by an Amata Dolerite [equivalent] dyke.|Grey, brown and white, laminated micaceous siltstone, overlain by grey and pink laminated dolostone, sometimes stromatolitic, and grey limestone. Typically unmetamorphosed, but locally to lower amphibolite grade.|12-JUL-16
15279|Pinyinna beds|69673|5|Briefly described|p63, p80, p84, p88, p91|Neoproterozoic|Neoproterozoic|||||Overlies Dean Quartzite, correlated with Bitter Springs Formation|Micaceous siltstone overlain by laminated dolostone, sometimes stromatolitic; some limestone.|
15279|Pinyinna beds|70416|6|Mentioned|p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
15279|Pinyinna beds|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15279|Pinyinna beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, sandstone, siltstone, phyllite|
15279|Pinyinna beds|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Grey quartz-muscovite phyllite, crystalline dolostone, fine-grained sandstone, red, green and pale grey fissile siltstone, dolomitic siltstone. Dominated by phyllite, interlayered with dolostone and minor schists in the north and Petermann Ranges.|
15279|Pinyinna beds|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||||
15279|Pinyinna beds|73085|6|Mentioned|p1|Tonian|Tonian|[Written as PINYINNA BEDS].||||Underlain by Dean Quartzite. Equivalent to Bitter Springs Group.||
15279|Pinyinna beds|73086|5|Briefly described|p: 3, 7, 15, 18, 30, 39, 148, 151, 154|||Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Restricted to sporadic exposures in the southwest of the basin. May correlate specifically with the Gillen Formation because of the conformable to transitional basal boundary with quartzite units.||||Correlates to Bitter Springs Group. Conformably underlain by Dean Quartzite|Shale and grey, crystalline, laminated, foetid and stromatolitic dolostone.|
15284|Pioneer Sandstone|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, dolomite, minor conglomerate.||||||
15284|Pioneer Sandstone|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Cryogenian|||||||
15284|Pioneer Sandstone|22560|6|Mentioned|p2|||||||||
15284|Pioneer Sandstone|22561|6|Mentioned|p16|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22566|5|Briefly described|p81|||See Pioneer Formation - p81.||||||23-NOV-06
15284|Pioneer Sandstone|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22648|4|Described|p 135|||Type section in Ellery Creek p 127.  Overlain by [??check!] Areyonga Formation, p135.||||||18-APR-18
15284|Pioneer Sandstone|22649|4|Described|p 145|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|In the Amadeus Basin.||||||17-JAN-07
15284|Pioneer Sandstone|22826|4|Described|p570|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|22901|6|Mentioned|75|||Geological province: Amadeus Basin.||||||23-NOV-06
15284|Pioneer Sandstone|22907|6|Mentioned|42|||||||||
15284|Pioneer Sandstone|23287|6|Mentioned|Fig.4|||Age: Upper Cryogenian. of Amadeus Basin.||||||
15284|Pioneer Sandstone|23314|5|Briefly described|333 Fig.4|Neoproterozoic III||In the Amadeus Basin.||||||16-NOV-06
15284|Pioneer Sandstone|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Cryogenian|||||||
15284|Pioneer Sandstone|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||
15284|Pioneer Sandstone|24301|5|Briefly described|p16|||Geological Province: Amadeus Basin||||||
15284|Pioneer Sandstone|35805|6|Mentioned|Fig.3|||||||||
15284|Pioneer Sandstone|35863|6|Mentioned|Table 1|||||||||
15284|Pioneer Sandstone|37928|5|Briefly described|p516|||||||||
15284|Pioneer Sandstone|37929|6|Mentioned|Fig.2|||||||||
15284|Pioneer Sandstone|38157|6|Mentioned|Table VI|||||||||
15284|Pioneer Sandstone|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|38945|6|Mentioned|p130|||||||||
15284|Pioneer Sandstone|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, feldspathic sandstone; minor granule conglomerate. Geological Province: Amadeus Basin.||||||14-FEB-06
15284|Pioneer Sandstone|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15284|Pioneer Sandstone|40740|3|Fully described|p88|||Described p12.||||||23-NOV-06
15284|Pioneer Sandstone|40906|6|Mentioned|Fig.9|||||||||
15284|Pioneer Sandstone|41405|6|Mentioned|p205|||||||||
15284|Pioneer Sandstone|41852|6|Mentioned|p220|||||||||
15284|Pioneer Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
15284|Pioneer Sandstone|42504|5|Briefly described|p72|||||||||
15284|Pioneer Sandstone|42643|6|Mentioned|Fig.4 P19|||||||||
15284|Pioneer Sandstone|42886|6|Mentioned|p217|||Of Preiss (1978). Upper part of Areyonga Formation of Prichard and Quinlan (1962). Correlated with Olympic Formation.||||||17-JAN-07
15284|Pioneer Sandstone|42940|5|Briefly described|Plate 9|||||||||
15284|Pioneer Sandstone|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
15284|Pioneer Sandstone|43503|6|Mentioned|12-50|||Age from Ediacaran.||||||23-NOV-06
15284|Pioneer Sandstone|43756|6|Mentioned|p542|||||||||
15284|Pioneer Sandstone|44111|6|Mentioned|p.58, Fig. 2|||in Amadeus Basin. Presented as "Pioneer" only in Fig. 2.||||||
15284|Pioneer Sandstone|45155|6|Mentioned|p28|||Correlation||||||
15284|Pioneer Sandstone|46730|5|Briefly described|p7|||Overlain by Pertatataka Formation. Underlain by Bitter Springs Formation. Geological Province: Amadeus Basin||||||17-JAN-07
15284|Pioneer Sandstone|46865|2|Defined|p57|late Adelaidean|late Adelaidean|||||||
15284|Pioneer Sandstone|49796|5|Briefly described|p1 & Sections|||||||||
15284|Pioneer Sandstone|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Pebble to cobble conglomerate with carbonate matrix.||||||07-FEB-11
15284|Pioneer Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
15284|Pioneer Sandstone|61732|3|Fully described|p4 Fig. 3, p92-93, p102|Cryogenian|Cryogenian|Of Olympic Fm. Unconformable on Bitter Springs Fm; elsewhere overlies or interfingers with Olympic Fm. Cap dolostone rocks (or 'upper cap dolomite' of Preiss et al (1978)) are overlain by the Pertatataka Fm. See also p5 Tb. 1, p31, p87.||||||07-FEB-11
15284|Pioneer Sandstone|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
15284|Pioneer Sandstone|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
15284|Pioneer Sandstone|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Amadeus Basin.||||||
15284|Pioneer Sandstone|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||||Pebble to cobble conglomerate with carbonate matrix.|
15284|Pioneer Sandstone|63562|6|Mentioned|p338 fig 3,p343, p346 fig 8,p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin. Called Pioneer Formation on p343.||||Is overlain by Pertatataka Formation.|Conglomerates and arkosic sandstones interpreted as glacial outwash deposits.|
15284|Pioneer Sandstone|64068|6|Mentioned|p46|||Amadeus Basin. Correlated with Sun Hill Arkose, Little Burke Tillite, Black Stump Arkose, Wonnadinna Dolostone, Oorabra Arkose, Boko Formation, southern Georgina Basin.||||||
15284|Pioneer Sandstone|64103|6|Mentioned|p404|||Geological Province: Amadeus Basin.||||||07-FEB-11
15284|Pioneer Sandstone|64625|5|Briefly described|p243-245, p248-253, p256-258|Neoproterozoic|Neoproterozoic|Amadeus Basin. Near-shore deposits. Lithology, C and O isotopes detailed.||||Unconformably overlies Aralka Formation. Disconformably overlies Bitter Springs Formation. Unconformably overlain by Gaylad Sandstone, overlain by Pertatataka Formation|Fenestrate-carbonate clast breccia, dolomitic quartz sandstone and chert pebble conglomerate.|
15284|Pioneer Sandstone|64778|6|Mentioned|p18|||Amadeus Basin. Thermal and maturation history modelling.||||||
15284|Pioneer Sandstone|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
15284|Pioneer Sandstone|64809|6|Mentioned|p3 Fig.2, p6 Fig.4, p11 Fig.10.|Proterozoic|Proterozoic|See also p13 Fig.13.||||||
15284|Pioneer Sandstone|65233|3|Fully described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Tog. with lateral equiv.Olympic Fm. disconformable on Aralka Fm. Geol.prov: Amadeus Basin. Consists of intertidal sandstone capped by 'marker' dolostone in western part of basin - correlated with Marinoan Nucaleena Dolostone in Adelaide Geosyncline.||||||07-FEB-11
15284|Pioneer Sandstone|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
15284|Pioneer Sandstone|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Amadeus Basin||||||
15284|Pioneer Sandstone|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Amadeus Basin||||||
15284|Pioneer Sandstone|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3.||||||
15284|Pioneer Sandstone|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Olympic Formation. Is overlain unconformably by Pertatataka Formation.||
15284|Pioneer Sandstone|67856|6|Mentioned|p345 fig 4-34, p337, p338 fig 4-30|Neoproterozoic|Neoproterozoic|Shown as equivalent to Olympic Formation.||||||
15284|Pioneer Sandstone|68270|4|Described|p679,682-688|Cryogenian|Cryogenian|Amadeus Basin. Type section occurs in Ellery Creek, 1.0-1.3 km south of contact with basement; lat. 23'47'24"S, long.133'04'12"E. Crops out mainly in the N-NE Amadeus Basin (Preiss et al. 1978; Shaw & Wells 1983; Field 1991; Freeman et al. 1991; Williams et al. 2007), but a 9 m section was intersected in Wallara 1 in the central part of the basin (Indigo Oil & Sirgo Exploration 1990), real extent is unknown. Less than 170m thick. Glacial outwash fan deposit. Includes a paraconformable "upper marker cap dolomite" that resembles that in Wahlgu Formation and is related to Elatina glaciation. Contains columnar stromatolite Anabaria = Kotuikania juvensis (Elleria minuta), and could be used a straitgraphic marker in central Austtralian basins. Correlable to Elatina Formation, Nuccaleena Formation.||||Overlain by Pertatataka Formation, Underlain disconformably by Aralka Formation.|Mostly of feldspathic, medium- to coarse-grained, cross-bedded sandstone and conglomerate; dolomite and chert; minor lodestones.|03-JUL-19
15284|Pioneer Sandstone|68316|6|Mentioned|p778 Fig.1|||||||||
15284|Pioneer Sandstone|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15284|Pioneer Sandstone|68733|6|Mentioned|p188, p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.|||||Peri-glacial arkosic sandstone.|
15284|Pioneer Sandstone|69031|6|Mentioned|p4|||Amadeus Basin.||||||
15284|Pioneer Sandstone|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Aralka Formation. Is overlain by Pertatataka Formation. Is equivalent to Olympic Formation.|Conglomerate and sandstone.|12-JUL-16
15284|Pioneer Sandstone|69438|3|Fully described|p23:2-5, 7-8, 10, 15, 17-19, 55, 60|Ediacaran|Ediacaran|Priess et al. (1978). Central-northern Amadeus Basin. About 170m thick at the type section at Ellery Creek. Priess et al. (1978) reassigned the upper Member of the Areyonga Formation (Pritchard and Quinlan, 1962) to this unit. Drillhole Ooraminna-2 targeted this unit for gas.||||Disconformably overlies Areyonga Formation and Bitter Springs Formation. Lateral equivalent of Olympic Formation. Is overlain ?disconformably by Pertatataka Formation.|Cross-bedded medium- to coarse-grained feldspathic and arkosic sandstone, grading up-section to c.1m of pink-grey dolostone with red-brown chert nodules. The top is irregular with columnar stromatolites, pebbly sandstone and conglomerate.|12-JUL-16
15284|Pioneer Sandstone|69443|5|Briefly described|p28:8|||Adelaide Fold Belt. Glacigene and post-glacial deposits related to the Elatina (previously Marinoan) glaciation.||||Equivalent to Keepera Group (Georgina Basin).||12-JUL-16
15284|Pioneer Sandstone|69606|5|Briefly described|p3, p4 fig 2, p12, p14|Cryogenian|Cryogenian|Amadeus Basin. Potential reservoir and seal rock. Inferred to have been deposited during the Elatina glaciation.||||Overlies the Aralka Formation, inferred to be equivalent to the Olympic Formation.|Sandstone, conglomerate and diamictite.|
15284|Pioneer Sandstone|69673|5|Briefly described|p63, p65, p81, p84, p88, p91, p98, p101|||Reservoir rock, hosts Ooraminna gas field.||||Overlain by Gaylad Sandstone, Pertatataka Formation, overlies Olympic Formation, disconformably overlies Areyonga Formation|Cross bedded, medium to coarse grained feldspathic and arkosic sandstone, grading into thin dolostone with chert nodules.|
15284|Pioneer Sandstone|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p17, p20-22,p47-48|Neoproterozoic|Neoproterozoic|Central-northern Amadeus Basin. A potential equivalent to the Olympic Sandstone. Shallow-marine to tidal deposits. Likely zircon provenance discussed. Estimated age between ~640 Ma and ~580 Ma, based on correlations with other glacial successions, is considerably younger than the youngest detrital zircon.|709 +/- 15 Ma (maximum depositional age).|||Is overlain unconformably by Gaylad Sandstone. Lateral equivalent of Olympic Formation.|Medium- to coarse-grained, feldspathic and arkosic sandstone with common sedimentary structures. Dolomitic in upper parts. Pink dolostone and columnar stromatolites at top.|
15284|Pioneer Sandstone|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Equivalent to Olympic Formation. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation.||
15284|Pioneer Sandstone|70416|5|Briefly described|p63, p65, p68, p72-73|Cryogenian|Cryogenian|Deposited during the Elatina Glaciation. Contains erratics of Aralka Formation with stromatolites (described in great detail).||||Unconformably overlies Aralka Formation. Is overlain by Pertatataka Formation. Laterally equivalent to Olympic Formation.||
15284|Pioneer Sandstone|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Pertatataka Formation. Underlain by Aralka Formation. Equivalent to Olympic Formation.||
15284|Pioneer Sandstone|71080|5|Briefly described|p29 fig 20, p30, 31|Cryogenian|Cryogenian|Amadeus Basin. Supersequence 3. Significant gas flows in Ooraminna 1 and 2.|||||Diamictite, sandstone and lesser conglomerate?|
15284|Pioneer Sandstone|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
15284|Pioneer Sandstone|71279|5|Briefly described|p355 Fig.2, p365-368|Ediacaran|Ediacaran|Amadeus Basin.|||||Highly silicified sandstone, shale, dolostone.|
15284|Pioneer Sandstone|71344|6|Mentioned|p1094|||Amadeus Basin. Glacial.||||Equivalent to Olympic Formation.||10-NOV-17
15284|Pioneer Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|709+/-15 Ma (MDA: U-Pb zircon SHRIMP)||||Medium-grained sandstone.|
15284|Pioneer Sandstone|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Gaylad Sandstone or Pertatataka Formation. Equivalent to Olympic Formation. Grades into Inindia beds.||
15284|Pioneer Sandstone|72375|4|Described|p1-2,20,22-23,25|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Preiss et al., 1978. Extends across the north and northcentral Amadeus Basin, and can be correlated with Elatina glacial successions of the Adelaide Rift Complex and the Georgina, Ngalia and Officer basins (Lindsay 1993, Walter et al 1995). Interpreted to have been deposited in a shallow marine to tidal setting restricted to central-northern part of the Amadeus Basin (Preiss et al., 1978). Stratigraphic top of Pioneer Sandstone is characterised by irregular erosional surface containing erosional scours and filled with pink dolomite with columnar stromatolites (Normington et al., 2015). SHRIMP U-Pb zircon analysis by Kositcin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 709+\-15 Ma, which is older that the inferred depositional age of c. 640 to 580 Ma (see Williams 1998, Grey et al., 2011) based on stratigraphic equivalence to Olympic Formation. LA-ICP-MS Hf isotopic signatures for the zircon age populations from NTGS AS13CJE031 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p24 for Hf isotopic results and interpretations).||||Overlain unconformably by Gaylad Sandstone. Laterally correlable (interfingers with) to Olympic Formation.|Quartz sandstone, typically medium- to coarse-grained, feldspathic and arkosic with common sedimentary structures; overlain by dolomitic sandstone with abundant tabular cross-beds and, in parts, contains discrete dolostone.|
15284|Pioneer Sandstone|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Amadeus Basin. Age implied from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
15284|Pioneer Sandstone|72601|5|Briefly described|p3-5, p7-8, p11, p17|Cryogenian|Cryogenian|Amadeus Basin. Deposition was coeval with the Elatina glaciation. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Unconformably underlain by Aralka Formation. Overlain by Pertatataka Formation. Equivalent to Olympic Formation. Correlated to Cottons Breccia.||
15284|Pioneer Sandstone|73085|6|Mentioned|p1|Ediacaran|Ediacaran|[Unclear relationship with Olympic Formation].||||Underlain by[?] Aralka Formation. Partly overlain by Pertatataka Formation unconformably. Partly overlain by and equivalent to Gaylad Sandstone. Equivalent to Inindia beds.||
15284|Pioneer Sandstone|73086|2|Defined|[See comments].|Cryogenian|Cryogenian|[Defined herein. No revised definition card]. Glaciogenic. Amadeus Basin. Part of Supersequence III. Lateral equivalent of the Olympic Formation; more extensively recognised in the subsurface than Olympic Formation. Primarily a feldspathic and pebbly sandstone with common conglomerate low in the unit and dolostone higher in the unit; capped by pink, stromatolite-bearing dolostone (Elleria minuta). Named after Pioneer Creek. Type section: Ellery Creek (sometimes obscured by alluvium). Key localities: Ringwood (Gaylad Syncline); Hidden Valley (Ross River Syncline). Distribution: confined to the northeast and north central margin of the basin as thin, discontinuous intervals. Previously described as a member of the Areyonga Formation. Type section thickness: 170 m. Where visible, sandstone is poorly sorted and weakly cross-bedded including herringbone cross-beds in the upper portion. Clear and distinctive cap carbonate. Correlated with Marinoan glacial successions. Geochron from detrital zircon maximum depositional ages; also constrained by the ca 660-635 Ma Marinoan glaciation. Interpreted to be an intraglacial glacial outwash or periglacial facies that probably correlates with the Olympic Formation. Partly correlates to upper Inindia beds. Possibly correlates to Mount Doreen, Elatina, and Nuccaleena formations. Partly equivalent to 'Undoolya Sequence'. p: 3, 5-6, 18, 62-63, 79, 99-101, 112-118, 122-123, 143, 151, 157, 167.|709 +/- 14 Ma SHRIMP U-Pb|||Equivalent to Olympic Formation. Unconformably underlain by Bitter Springs Group, Areyonga and Aralka formations. Overlain by [and equivalent to?] Gaylad Sandstone. Overlain by Pertatataka Formation.|Dominantly white to brown, friable, medium- to coarse-grained, cross-bedded, feldspathic sandstone capped by pink stromatolite-bearing dolostone.|
15284|Pioneer Sandstone|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Unconformably underlain by Aralka Formation. Unconformably overlain by Pertatataka Formation. Equivalent to Gaylad Sandstone and Olympic Formation.||
15284|Pioneer Sandstone|73180|4|Described|p47-48, p51 Fig.6, p52-54|Neoproterozoic|Neoproterozoic|Amadeus Basin. Elatina glacial/post-glacial sequences. Outcrops around Mount Connor. Disconformable contact with Bitter Springs Group in the north and northeast of the basin from erosion by a grounded ice sheet, deposition of thin sandstones and conglomerates from localised high-energy deposition, likely glacial outwash. [Descriptions of the Olympic Formation were also applied to the Pioneer Sandstone in text].||||Equivalent to the Olympic Formation, disconformably overlies the Aralka Formation, conformably underlies the Pertatataka Formation.|Glacial/periglacial clastic deposits including diamictite and reworked carbonates interbedded and capped by a distinctive pink to buff dolostone in proximal glaciogenic deposits, commonly bearing diagnostic stromatolites.|
15284|Pioneer Sandstone|75070|5|Briefly described|p175, 178-184|Middle Ordovician|Middle Ordovician|Western Tasmania. Detrital zircon signature discussed. Detrital zircon graph. Hf isotope diagram.|||||Sandstone.|
15287|Pipeline Andesite|42221|6|Mentioned|Table 1 P6|||Reserved as Pipeline Andesite Member||||||
15287|Pipeline Andesite|42436|5|Briefly described|Fig.2 P.75|||||||||
15287|Pipeline Andesite|42696|6|Mentioned|Plate 1B|||||||||
15287|Pipeline Andesite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
15287|Pipeline Andesite|43101|6|Mentioned|p21|||of Black Flag Group||||||
15287|Pipeline Andesite|43162|6|Mentioned|5|||U-Pb age: 2704+/-8Ma||||||
15287|Pipeline Andesite|43496|6|Mentioned|12|||||||||
15287|Pipeline Andesite|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Of the Black Flag Group. Unconformably overlian by Kurrawang Formation. Geological Province: Ora Banda Domain.||||||07-FEB-11
15287|Pipeline Andesite|60627|5|Briefly described|p65 Tb.1|||Of the Black Flag Group.||||||
15287|Pipeline Andesite|65204|5|Briefly described|pg6 Tbl.1, 14|Neoarchean|Neoarchean|Of the Black Flag Group. Andesite lava, tuff, volcanic breccia. U-Pb zircon age of 2704+/-8Ma.||||||
15287|Pipeline Andesite|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.||Black Flag Group.||||
15292|Pirie Member|24455|5|Briefly described|p327|||Of the Cardabia Calcarenite.  Geological Province: Carnarvon Basin.||||||22-MAR-05
15292|Pirie Member|40617|6|Mentioned|p14|||||||||
15292|Pirie Member|41271|4|Described|p166|||||||||
15292|Pirie Member|61155|5|Briefly described|p15|Paleocene|Late Paleocene|Of the Cardabia Calcarenite. Geological Province: Carnarvon Basin/onshore.||||||
15310|Plantagenet Group|9173|5|Briefly described|Map legend.|Eocene|Eocene||||Includes Pallinup Siltstone and Werillup Formation.|||
15310|Plantagenet Group|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Includes Norseman Limestone, Werrilup Formation and Pidinga Formation.||||||07-FEB-11
15310|Plantagenet Group|22737|6|Mentioned|2,13,15|Late Eocene|Late Eocene|||||||
15310|Plantagenet Group|22814|5|Briefly described|fig2|Cenozoic|Cenozoic|||||||19-NOV-08
15310|Plantagenet Group|23331|4|Described|1088|||||||||10-SEP-09
15310|Plantagenet Group|23533|5|Briefly described|p561|Eocene|Eocene|Geological Province: Bremer Basin.||||||
15310|Plantagenet Group|23584|6|Mentioned|p29|||Geological Province: Bremer Basin.||||||
15310|Plantagenet Group|23727|5|Briefly described|p110|Late Eocene|Middle Eocene|||||||
15310|Plantagenet Group|23728|5|Briefly described|Map Legend|Tertiary|Tertiary|Geological Province Bremer Basin.||||||
15310|Plantagenet Group|23752|6|Mentioned|p18|||||||||
15310|Plantagenet Group|23753|5|Briefly described|Map legend|Tertiary|Tertiary|Includes the Pallinup Siltstone. Geological Province: Bremer Basin.||||||28-JUL-09
15310|Plantagenet Group|23754|5|Briefly described|Map Legend|Tertiary|Tertiary|Geological Province Bremer Basin.||||||
15310|Plantagenet Group|23817|5|Briefly described|p429|Tertiary|Tertiary|Geological Province: Bremer Basin.||||||
15310|Plantagenet Group|24094|5|Briefly described|p269|||Includes Pallinup Siltstone and Werillup Formation. Geological Province: Bremer Basin||||||16-MAR-05
15310|Plantagenet Group|24160|6|Mentioned|p117, p150.|Eocene|Eocene|Bremer Basin (onshore sequence). Local deposits of clay suitable for the brick industry.|||Includes Pallinup Siltstone.||Mudstone, siltstone.|
15310|Plantagenet Group|24165|5|Briefly described|p15, p49-51, p59-60, p67, p69, p73, p96|Eocene|Eocene|See also Plate 1. Cheyne Bay area, Bremer Basin. Target for heavy mineral exploration. Hosts lignite deposits. High potential for further spongolite extraction.|||Werillup Formation, Pallinup Siltstone.||Sandstone, siltstone and conglomerate; commonly lateritised or overlain by pisolitic scree.|
15310|Plantagenet Group|24410|5|Briefly described|p37, p82 Fig. 41|Tertiary|Tertiary|Includes the Pallinup Siltstone. In the Albany region of W.A. See also p87.||||||24-NOV-09
15310|Plantagenet Group|29601|6|Mentioned|p82|||||||||
15310|Plantagenet Group|29693|6|Mentioned|p86|||||||||
15310|Plantagenet Group|30144|4|Described|p82|||Tropical mangrove plant communities||||||
15310|Plantagenet Group|30185|6|Mentioned|p107|||Cyclammina incisa occurrence.||||||
15310|Plantagenet Group|30189|6|Mentioned|p132|||Consists of Werrillup and Pollinup Siltstone||||||
15310|Plantagenet Group|30268|6|Mentioned|p44|||||||||
15310|Plantagenet Group|30961|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15310|Plantagenet Group|30970|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15310|Plantagenet Group|30976|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
15310|Plantagenet Group|31049|6|Mentioned|p393|||See also P394||||||
15310|Plantagenet Group|31051|3|Fully described|Fig.1.|||||||||
15310|Plantagenet Group|31053|6|Mentioned|p545|||||||||
15310|Plantagenet Group|31054|6|Mentioned|Fig. 1|||||||||
15310|Plantagenet Group|31562|5|Briefly described|p13|||||||||
15310|Plantagenet Group|31913|6|Mentioned|p11|||Refs. Cockbain (1968)||||||
15310|Plantagenet Group|31922|6|Mentioned|p169|||||||||
15310|Plantagenet Group|32311|4|Described|p12|||||||||
15310|Plantagenet Group|32552|5|Briefly described|p66|||U.Eocene. See also P74, 131, 146, 156||||||
15310|Plantagenet Group|32648|6|Mentioned|p32|||Tertiary||||||
15310|Plantagenet Group|32743|6|Mentioned|p183|||||||||
15310|Plantagenet Group|32748|6|Mentioned|p19|||||||||
15310|Plantagenet Group|32750|4|Described|p306|||See P303. Refers Teichert (1944) & Clarke & Phillips (1954)||||||
15310|Plantagenet Group|33272|6|Mentioned|Fig.2|||||||||
15310|Plantagenet Group|33445|5|Briefly described|p33|||||||||
15310|Plantagenet Group|33801|6|Mentioned|p49|||||||||
15310|Plantagenet Group|34102|6|Mentioned|p52|||||||||
15310|Plantagenet Group|34103|6|Mentioned|p92|||||||||
15310|Plantagenet Group|35381|6|Mentioned|p188|||Also shown on Fig.1||||||
15310|Plantagenet Group|35617|6|Mentioned|p370|||Location of chert.||||||
15310|Plantagenet Group|36200|6|Mentioned|p5|||||||||
15310|Plantagenet Group|36257|6|Mentioned|Table 2.1|||||||||
15310|Plantagenet Group|36305|6|Mentioned|p354|||||||||
15310|Plantagenet Group|36890|3|Fully described|p429|||Formerly Plantagenet Beds.||||||15-DEC-08
15310|Plantagenet Group|37062|6|Mentioned|p186|||||||||
15310|Plantagenet Group|37134|5|Briefly described|p372|||||||||
15310|Plantagenet Group|37341|4|Described|p233|||||||||
15310|Plantagenet Group|37350|6|Mentioned|Fig.1|||||||||
15310|Plantagenet Group|37596|6|Mentioned|p79|||||||||
15310|Plantagenet Group|38214|5|Briefly described|p241|||||||||
15310|Plantagenet Group|38578|4|Described|p25|||||||||
15310|Plantagenet Group|38773|6|Mentioned|p44|||||||||
15310|Plantagenet Group|39167|6|Mentioned|p68|||||||||
15310|Plantagenet Group|39173|6|Mentioned|p325|||||||||
15310|Plantagenet Group|39794|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15310|Plantagenet Group|39795|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15310|Plantagenet Group|40148|6|Mentioned|p161|||||||||
15310|Plantagenet Group|40358|6|Mentioned|p23|||||||||
15310|Plantagenet Group|40877|5|Briefly described|p55|||||||||
15310|Plantagenet Group|40928|6|Mentioned|p13|||||||||
15310|Plantagenet Group|40932|6|Mentioned|p16|||||||||
15310|Plantagenet Group|40992|6|Mentioned|Fig.23|||||||||
15310|Plantagenet Group|41517|6|Mentioned|Fig.3|||||||||
15310|Plantagenet Group|41626|6|Mentioned|p50|||||||||
15310|Plantagenet Group|41771|6|Mentioned|p49|||||||||
15310|Plantagenet Group|42424|5|Briefly described|p3|||||||||
15310|Plantagenet Group|42473|6|Mentioned|p13|||||||||
15310|Plantagenet Group|42535|6|Mentioned|p17|||||||||
15310|Plantagenet Group|42817|5|Briefly described|p29|||see also Fig.6||||||
15310|Plantagenet Group|42959|5|Briefly described|p58 Fig.3|||||||||
15310|Plantagenet Group|43189|5|Briefly described|Map Legend||Tertiary|||||||
15310|Plantagenet Group|43203|5|Briefly described|Map Legend||Eocene|Bremer Basin||||||
15310|Plantagenet Group|43212|5|Briefly described|p6||Eocene|||||||
15310|Plantagenet Group|43283|5|Briefly described|Map Legend||Tertiary|||||||
15310|Plantagenet Group|43305|5|Briefly described|Map Legend||Tertiary|||||||
15310|Plantagenet Group|43311|5|Briefly described|Map Legend||Tertiary|||||||
15310|Plantagenet Group|43498|5|Briefly described|8||Late Eocene|||||||
15310|Plantagenet Group|43672|6|Mentioned|p330||Eocene|||||||
15310|Plantagenet Group|43721|6|Mentioned|p29|||||||||
15310|Plantagenet Group|44145|6|Mentioned|p556|Late Eocene|Late Eocene|Clastic deposition, primarily in coastal swamps. Western margin of Eucla Basin.||||||
15310|Plantagenet Group|44146|5|Briefly described|p561-563|Late Eocene|Eocene|Bremer Basin. Described as Middle to Late Eocene age.|||Includes Pallinup Sandstone, Werillup Formation.|||
15310|Plantagenet Group|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Comprises Werillup Formation, [Norseman Limestone Formation?] and Pallinup Siltstone. Includes bryozoal carbonates and spongolites. Age: 51.5-36.5Ma. Geological Province: Bremer Basin and Norseman region.||||||
15310|Plantagenet Group|62381|5|Briefly described|p9.|Eocene|Eocene|Onshore Bremer Basin. Very shallow dip to the south; infills paleodrainage and depressions. Is overlain around the coast by locally cross-bedded, carbonate-cemented arenites.|||Includes Pallinup Siltstone and Werillup Formation.||Sandstone and siltstone.|
15310|Plantagenet Group|64580|6|Mentioned|map legend|||||||||
15310|Plantagenet Group|65414|6|Mentioned|p111.|Eocene|Eocene||||Includes Werillup Formation and Pallinup Siltstone.|||
15310|Plantagenet Group|65487|6|Mentioned|p2|||Cenozoic cover group omitted from the interpreted bedrock geology map associated with record 2007/13.||||||
15310|Plantagenet Group|68811|6|Mentioned|p102, p189 tbl 44|Tertiary|Tertiary||||Includes the Werillup Formation and the Pallinup Sandstone/Siltstone.|||16-APR-20
15310|Plantagenet Group|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Eocene|Eocene||||Includes Pallinup Formation.|||
15310|Plantagenet Group|69598|5|Briefly described|p2, p9, p11, p11 Tb.1, p29 Tb.4|Late Eocene|Middle Eocene|Eucla Basin. Up to 60m thick.|||Includes the Werrilup and Pallinup Formations.|Overlies the Eundynie Group.||
15310|Plantagenet Group|70802|5|Briefly described|GEOL_LUT_CSV files|||Of Eucla Basin. See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv.|||Includes Pallinup Formation.|||
15310|Plantagenet Group|70826|6|Mentioned|p7 tbl 4|Eocene|Eocene|Eucla Basin.||||||
15310|Plantagenet Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
15310|Plantagenet Group|71270|5|Briefly described|GEOL_LUT_CSV files|||Of Eucla Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||Includes Pallinup Formation.|||
15310|Plantagenet Group|71787|14|Not recorded|p95-96 ||Late Eocene|Upper Eocene.||||||
15310|Plantagenet Group|71788|14|Not recorded|p97-98 ||Late Eocene|Upper Eocene||||||
15310|Plantagenet Group|71789|2|Defined|p99-101||Late Eocene|Pallinup Siltstone and Werillup Formation defined pp 99 & 100.||||||
15310|Plantagenet Group|72034|5|Briefly described|500k_interpgeop16_lut|Priabonian|Bartonian|Eucla Basin. Age from biostratigraphy.|||||Siltstone, spongolite, sandstone, lesser limestone; lignite in lower part.|
15330|Plover Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p216|Middle Jurassic|Early Jurassic|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
15330|Plover Formation|7142|6|Mentioned|p350 Fig.4.|Middle Jurassic|Early Jurassic|Browse Basin.||||Overlies Nome Formation. Is overlain by Lower Vulcan and Montara Formations.||
15330|Plover Formation|12466|6|Mentioned|p177 Fig.10.|||||||Overlies Mount Goodwin Formation. Is overlain by Flamingo Group.||
15330|Plover Formation|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Callovian|Jurassic|Type Section: Petrel 1 well (1820-2229m). 200-672m thick non-marine to marginal marine sediments.||Troughton Group||Overlies Malita Formation. Overlies Cape Londonderry Formation (disconformably). Overlain by Frigate Shale (uncf).|Coarse grained sandstone; minor shale, coal and limestone.|
15330|Plover Formation|13222|6|Mentioned|p234.|Early Jurassic|Early Jurassic|This unit was not involved in compressive structures, and truncates older structures within the Triassic. Hence folding (and formation of anticlinal traps) is constrained to late Triassic-Early Jurassic.||||||
15330|Plover Formation|13224|5|Briefly described|p484|Oxfordian|Pliensbachian|||||||
15330|Plover Formation|13234|5|Briefly described|p250 Fig.2, p260, p263 Tb.4. |Middle Jurassic|Middle Jurassic|Coastal plain deposits at the top of this unit provide reservoir facies.||||Is overlain by Flamingo Group.|Includes fluvial and paralic sands.|
15330|Plover Formation|13267|5|Briefly described|pp273-286.|Middle Jurassic|Middle Jurassic|Sahul Platform, Bonaparte Basin. Fair to excellent hydrocarbon reservoir quality. Variable oil shows observed. Hydrocarbon-charged fluid entering the lower part of this fluvio-deltaic unit was silica-rich (oil inclusions).||||Is overlain by Elang Formation.|Quartzose, medium- to coarse-grained, moderately well-sorted sandstone with minor amounts of clay allowing extensive quartz overgrowth, reducing porosity; minor coal.|
15330|Plover Formation|13310|6|Mentioned|p295.|Middle Jurassic|Middle Jurassic|Presence of a single palaeo-oil column from Octavius 2 exploration well, Vulcan Sub-basin.|||||Sandstones.|
15330|Plover Formation|13353|6|Mentioned|p401 Fig.2.|||||||Is overlain by Lower Vulcan and Montara Formations.||
15330|Plover Formation|13354|6|Mentioned|p375 Fig.6.|Middle Jurassic|Early Jurassic|Unit of Troughton Group. Overlies Nome Formation and underlies Lower Vulcan Formation.||86||||28-OCT-14
15330|Plover Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Jurassic|||||||01-MAR-10
15330|Plover Formation|23376|4|Described|p229 Fig.2;p227-9,235,240,244-5|Callovian|Hettangian|In the Bonaparte Basin.||||||23-NOV-06
15330|Plover Formation|23377|4|Described|p212 Fig.5; p211, 223|Late Jurassic|Early Jurassic|Unconformities at top and base. In the Vulcan Sub-basin.||||||23-NOV-06
15330|Plover Formation|23378|4|Described|p180 Fig.2, p177-179|Middle Jurassic|Early Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
15330|Plover Formation|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
15330|Plover Formation|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
15330|Plover Formation|24207|5|Briefly described|p209 Fig. 5, p210 Fig. 6|Toarcian|Toarcian|||||||01-MAR-10
15330|Plover Formation|24234|5|Briefly described|p287 Fig.3|Jurassic|Jurassic|Overlain by the Elang Formation. Geological Province: Bonaparte Basin.||||||17-MAR-05
15330|Plover Formation|24235|5|Briefly described|p298, p299|Jurassic|Jurassic|See also Plover formation. Geological Province: Bonaparte Basin.||||||
15330|Plover Formation|24427|5|Briefly described|p48, p49 Fig.2|Middle Jurassic|Early Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
15330|Plover Formation|24569|5|Briefly described|p248 Fig. 3|Oxfordian|Early Jurassic|Of the Troughton Group. Geological Province: Petrel Sub-basin.||||||17-MAR-05
15330|Plover Formation|41459|6|Mentioned|Fig.2|||||||||
15330|Plover Formation|41532|3|Fully described|p304|||||||||
15330|Plover Formation|41690|5|Briefly described|p6|||See also p57.||||||23-NOV-06
15330|Plover Formation|41731|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|41733|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|41759|6|Mentioned|p270|||||||||
15330|Plover Formation|42034|4|Described|Fig.4 P11|||||||||
15330|Plover Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
15330|Plover Formation|42056|4|Described|p98|||||||||
15330|Plover Formation|42057|4|Described|p75|||See also p79.||||||23-NOV-06
15330|Plover Formation|42066|6|Mentioned|Fig.3 P199|||||||||
15330|Plover Formation|42081|5|Briefly described|Fig.2 P291|||||||||
15330|Plover Formation|42151|6|Mentioned|Fig.3 P57|||||||||
15330|Plover Formation|42442|3|Fully described|p24|Callovian|Pliensbachian|NT and WA.||||||23-NOV-06
15330|Plover Formation|42861|5|Briefly described|p3|||||||||
15330|Plover Formation|43230|5|Briefly described|p9|Middle Jurassic|Early Jurassic|||||||03-SEP-14
15330|Plover Formation|43661|6|Mentioned|Fig.3|||||||||
15330|Plover Formation|43699|5|Briefly described|p3-4|Middle Jurassic|Early Jurassic|||||||
15330|Plover Formation|43739|6|Mentioned|p10||Middle Jurassic|||||||
15330|Plover Formation|43825|6|Mentioned|p147||Jurassic|||||||
15330|Plover Formation|43826|6|Mentioned|Fig.2,p163|Middle Jurassic|Early Jurassic|||||||01-MAR-10
15330|Plover Formation|43828|6|Mentioned|p206|||||||||
15330|Plover Formation|43829|5|Briefly described|Fig.2,p225||Middle Jurassic|In the Sahul Syncline.||||||23-NOV-06
15330|Plover Formation|49637|5|Briefly described|Fig.3|Middle Jurassic|Middle Jurassic|Of the Troughton Group. Geological Province: Londonderry High.||||||07-FEB-11
15330|Plover Formation|50027|5|Briefly described|p10|Middle Jurassic|Early Jurassic|Fluviodeltaic sands.  Geological Province: Browse Basin.||||||
15330|Plover Formation|60378|4|Described|p95-101, 104-120|Middle Jurassic|Early Jurassic|Marine to terrestrial sediments including coal-rich layers. Petroleum reservoir. Thickness variations and distribution discussed.|||||Fluvial to deltaic sandstone.|
15330|Plover Formation|60386|6|Mentioned|p300, 302, 314|Middle Jurassic|Early Jurassic|Browse Basin/Bonaparte Basin. Non-marine, deltaic-nearshore-shelf.||||||
15330|Plover Formation|60634|5|Briefly described|p1166, p1167 Fig.2,  p1168 Fig.3.|Late Jurassic|Early Jurassic|Hydrocarbon reservoir sealed by Early Cretaceous calcareous shales. Leakage from the Skua oil field is primarily controlled by a fault intersection.||Unit in Troughton Group.||Unconformably overlies Nome Formation. Is overlain by Vulcan Formation.|Sandstones.|
15330|Plover Formation|61250|5|Briefly described|p45|Middle Jurassic|Early Jurassic|The dominant source for the Laminaria and Corallina Oil fields.||||||
15330|Plover Formation|61548|6|Mentioned|p480 Fig.3|Middle Jurassic|Late Triassic|Northern Bonaparte Basin.||||||
15330|Plover Formation|61550|5|Briefly described|p494, p495 Fig.2, p505.|Middle Jurassic|Early Jurassic|Vulcan Sub-basin. Fluvio-deltaic mudstones. Contains oils and condensates for the Montara and Bilyara wells, modelled to have had late oil generation and charge in the Pliocene (5 Ma to present).||||Unconformably overlies Sahul Group. Is overlain unconformably by Swan Group.|Fluvio-deltaic mudstones.|
15330|Plover Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Early Jurassic|Of the Troughton Group.  Age: ~203-~154Ma. Geological Province:  Northern Bonaparte Basin, Petrel Sub-basin (offshore) and Money Shoals Basin.||||||01-MAR-10
15330|Plover Formation|63062|4|Described|p9 Fig. 9, p33|Middle Jurassic|Early Jurassic|Represents youngest component of the Troughton Group in the study area. Geological Province: Bonaparte, Arafura and Money Shoal Basins. Fine- to coarse-grained sandstones with interbedded siltstones and claystones, and minor coal; fluvial in origin.||||||07-FEB-11
15330|Plover Formation|63358|5|Briefly described|p4 Fig. 1.3|Callovian|Sinemurian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
15330|Plover Formation|64689|5|Briefly described|p3-18 |Middle Jurassic|Early Jurassic|Established as a regional oil and gas-liquids source rock: the dominant source for the Laminaria and Corallina oil fields; also as a target reservoir. Upper surface is the Callovian Unconformity.||||Unconformably overlies Nome Formation. Is overlain unconformably by Lower Vulcan Formation.||
15330|Plover Formation|64695|6|Mentioned|p265, p266, p267-269 Figs.12-14||||||||Sandstones.|
15330|Plover Formation|64696|5|Briefly described|p125; 127-128 Figs.2,3,4|Middle Jurassic|Early Jurassic|See also p129-131, p134-140. Bonaparte Basin. A key pre-rift reservoir/source unit.||||Unconformably overlies Nome Formation. Unconformably underlies the Vulcan Formation.|Basal red-bed succession of upward-fining channel sandstones capped by red/grey-green shales and siltstones; massive sandstones; coastal plain/deltaic shales; massive sheet-like sandstones.|
15330|Plover Formation|64697|5|Briefly described|p85, p86, p88, p96|Middle Jurassic|Early Jurassic|||||||
15330|Plover Formation|66187|5|Briefly described|p413 Fig.2|Middle Jurassic|Early Jurassic|Underlies the Montara Formation, overlies the Nome Formation. Mount Ashmore Dome.||||||
15330|Plover Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes yellow fine-grained sandstone; grey siltstone, mottled (bioturbated).|04-JAN-23
15330|Plover Formation|67200|5|Briefly described|app 2 p7||||||||Fine grained sandstone and siltstone; bioturbated.|
15330|Plover Formation|67370|6|Mentioned|p323 Fig.14.|Jurassic|Jurassic|Southeastern Bonaparte Basin. Type section in Petrel-1 between 2,229 - 2471 m.||||Overlies Malita Formation.||
15330|Plover Formation|68054|6|Mentioned|p41, 44, 49|Middle Jurassic|Early Jurassic|Bonaparte Basin. Penetrated by the Sunrise-2 and Sunset West-1 well; palynomorphs therein are a focus of this article. Abundant photographs; systematic palaeontology of dinoflagellate cysts.|||||Fluvial sandstones dominate the lower pars of this unit; shallow-marine sandstones in the upper.|
15330|Plover Formation|68135|5|Briefly described|p51, p61|Middle Jurassic|Early Jurassic|Bonaparte and Browse Basins.||Troughton Group.||Overlies Malita Formation.||14-SEP-17
15330|Plover Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Middle Jurassic|Early Triassic|||||||06-SEP-18
15330|Plover Formation|69297|4|Described|p283,  p285, p289|Middle Jurassic|Lower Jurassic|Money Shoal Basin and Barcoo and Seringapatam Sub-basins of the Browse Basin. Deposited in a fluvial-deltaic environment. Potential oil and gas source rocks. See also p303, p305, p307, p308, p309, p311, p320, p322, p324.||Troughton Group||Unconformably overlain by the Flamingo Group or the Montara Formation.|Coarsening upwards sandstones, interbedded with fine-grained beds of siltstone and shale.|
15330|Plover Formation|69418|6|Mentioned|p3:24, 26|||Pine Creek Orogen. Appears as ?Plover Formation eq. Identified as Petrel Formation in Sullivan (1970), hosts the Daly River Road surficial Fe deposit (described). Similarly identified as Petrel Formation in Ferenczi (2001), hosts the McLeans surficial-type Mn deposit (briefly described).||||||12-JUL-16
15330|Plover Formation|69452|5|Briefly described|p36:8, 15, 21, 28-29|Middle Jurassic|Early Jurassic|Petrel Sub-basin, Bonaparte Basin. Up to 500m thick (offshore). Drillhole Jabiru-1A intersected a 57m gross oil column in this unit and basal Flamingo Group, starting the Jabiru oil field. Also contained seven reservoir units in the Skua oil field.||Troughton Group.||||12-JUL-16
15330|Plover Formation|69455|6|Mentioned|p39:5|||||||Is overlain by Darwin Formation.||12-JUL-16
15330|Plover Formation|69456|4|Described|p40:1-5, 15|Early Cretaceous?|Early Jurassic|Bonaparte and Money Shoal Basins. In the NT, rocks of this unit are consistently referred to as "Plover Formation equivalent" (to the Bonaparte Basin succession). Onshore exposures were previously referred to as Petrel Formation (eg Pietsch and Stuart-Smith, 1987); that name was abandoned by Mory (1991) as it included an unconformity. Thickness is up to 564m offshore, where its age is given as late Early to late Middle Jurassic; and a queried assignation of up to 5m onshore, where its age is Jurassic to early Cretaceous. Fluvial braided-river systems to shallow-marine. Fair to very good petroleum source potential. Reservoir for gas accumulations in the E Bonaparte Basin.||Troughton Group.||Unconformably overlies Kulshill, Arafura and Goulburn Groups. Is overlain unconformably by Flamingo and Bathurst Island Groups.|(Offshore): Fine- to coarse-grained sandstone interbedded with siltstone and claystone, and minor coal. ?(Onshore): friable, poorly sorted, commonly limonitic sandstone and minor conglomerate.|12-JUL-16
15330|Plover Formation|69653|5|Briefly described|p1, 6, 8, 10, 15, 17-18, 37, 39, 43, 76|Middle Jurassic|Early Jurassic|Petrel Sub-basin. Suitable for CO2 storage; sealed by Frigate Shale. Delta plain- shoreface and fluvial deposits. Composite well diagram. Photomicrographs. See also p45-47, 50, 53, 63-64, 74.||Troughton Group.||Overlies Malita Formation. Is overlain by Elang Formation.|Mudstone; siltstone interbedded with fine-grained sandstone; massive pebbly sandstone; fine- to coarse-grained sandstone; very fine- to fine-grained sandstone. Facies described in detail.|
15330|Plover Formation|69673|5|Briefly described|p173||||||||Sandstone, siltstone and shale.|
15330|Plover Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Overlies Nome Formation. Is overlain by Montara Formation.||
15330|Plover Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Middle Jurassic|Early Jurassic|See also Regional geology: Figs.6-7, p5, p9-10, p12-15, p18-19. Sahul: Fig.2, p1-3. Vulcan: Fig.2, p1-2. Thick, widespread succession of fluvial and coastal plain sediments across most of the Bonaparte Basin (except the Ashmore Platform and the crest of the Londonderry High). A major source and productive (Skua and Jabiru fields) reservoir unit in the N Bonaparte Basin. Source and reservoir rocks in Sahul Syncline and Vulcan Sub-basin, and intraformational seal in the former.||Troughton Group.||Overlies Malita Formation. Is overlain by Elang Formation.|Includes local, thin, high-quality coals and pro-delta shales with high source potential.|12-JUL-16
15330|Plover Formation|70064|5|Briefly described|Northern Fig.2;p1-3. Yampi: Fig.2;p1-2|Bathonian|Hettangian|See also Regional: Fig. 6; p4-10. Central: Fig.2; p1-2. Browse Basin. Contains organic-rich rocks with fair to moderate oil potential, as well as gas-prone, high-quality coals and pro-delta shales. Potential reservoirs in horsts and tilted fault-blocks; sealed by Lower Vulcan Formation. Hosts gas in the Crux structure within the Heywood Graben. Has potential for intraformational seals.||Troughton Group.||Overlies Nome Formation (Sahul Group). Is overlain by Lower Vulcan Formation or Montara Formation (Swan Group).|Syn-rift sediments comprising fine- to very fine-grained sandstones, interbedded with occasional medium- to coarse-grained sandstones, siltstones, claystones and minor coals. Some local tuffaceous volcanics.|12-JUL-16
15330|Plover Formation|70098|5|Briefly described|p19 Fig.5|Middle Jurassic|Early Jurassic|||Troughton Group||Overlies Kulshill Group (and equivalent?). Is overlain by Flamingo Group, Lower (Flamingo Group).||
15343|Plumridge Formation|24347|5|Briefly described|p114|||||||||
15343|Plumridge Formation|41751|6|Mentioned|p9|||||||||
15343|Plumridge Formation|44145|4|Described|p550 tab 4-27, p556-7, p555 fig 4-194|Early Miocene|Early Miocene|Northern margin Eucla Basin. Unfossiliferous. Max exposed thickness 9 m. Max thickness estimated 100m. Age from stratigraphic relationships. Type section in Plumridge 1:250 000 sheet area 29deg43' S, 125deg04' E||||Grades laterally into Colville Sandstone.|Fine-grained sandstone, siltstone, claystone with intercalated pebbly sandstone with silcrete clasts.|08-OCT-15
15343|Plumridge Formation|69152|5|Briefly described|1m_geologyp08_lut.csv|Middle Miocene|Middle Miocene||||||Sandstone, siltstone, minor conglomeratic sandstone.|07-AUG-15
15343|Plumridge Formation|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|||Eucla Basin. Up to 9m thick. Potential carbon dioxide storage reservoir.||||Equivalent to the Colville Sandstone.  Grades into and interfingers with the Nullarbor Limestone.|Calcareous sandstone, minor siltstone, claystones and calcarenites.|
15343|Plumridge Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15343|Plumridge Formation|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton.|||||Sandstone, siltstone, minor conglomeratic sandstone|
15377|Point Maud Member|6944|5|Briefly described|p569, p574, p585 Table 1.|Late Devonian|Late Devonian|Member of Gneudna Formation. Vuggy and dolomitised limestone containing algal microfossils and possible Amphipora. Type section at Pendock 1D. Potential hydrocarbon reservoir.||||||23-SEP-15
15377|Point Maud Member|12471|6|Mentioned|p475 Fig.2, p483.|Late Devonian|Middle Devonian|Has excellent vuggy and cavernous porosity in Gascoyne Platform; its presence has yet to be demonstrated on the Peedamullah Shelf.||||||27-OCT-14
15377|Point Maud Member|12729|4|Described|p.14, 31; Fig.24||Devonian|Point Maud Formation of Geary, 1970. Deposition: reefal or platform facies. Identified on seismic sections as interval with few internal reflections in comparison to surrounding overlying strata. 320-331 m thick in drillhole intersections.||Gneudna Formation|||Massive dolomite. Core sample: Light grey to white dolomite with abundant vuggy and intercrystalline porosity and stylolites.|
15377|Point Maud Member|12731|6|Mentioned|p596.|||Has vuggy cavernous porosity, thus a potential hydrocarbon reservoir.||||||27-OCT-14
15377|Point Maud Member|14228|5|Briefly described|p7, p18, p19|Devonian|Devonian|Up to 331m thick. Dolomitization appears to have enhanced development of vuggy porosity and permeability.||Gneudna Formation|||Massive dolomite. Vuggy porosity and permeability.|
15377|Point Maud Member|23726|6|Mentioned|p29|||Geological Province: Carnarvon Basin.||||||
15377|Point Maud Member|40617|5|Briefly described|p15|||||||||
15377|Point Maud Member|41438|6|Mentioned|p102|||||||||
15377|Point Maud Member|42030|6|Mentioned|p744|||||||||
15377|Point Maud Member|42116|5|Briefly described|p22|||||||||
15377|Point Maud Member|60384|6|Mentioned|p260 table 2|||Of Nannyarra Sandstone? Shown from 1969 well Pendock-1||||||
15377|Point Maud Member|60725|6|Mentioned|p35 Fig.5. |||||||||
15377|Point Maud Member|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.||Gneudna Formation.|||Includes tan coloured limestone; vugs/borings rare to ubiquitous.|23-DEC-22
15377|Point Maud Member|67200|5|Briefly described|p18 table 1, p47, p51, p55, app 2 p6|||Thermal conductivity of 5.00 W/mK||Gneudna Formation|||Vuggy limestone,vuggy and porous dolostones.|
15385|Point Waylen beds|41278|6|Mentioned|Fig.4|||||||||
15386|Poison Hill Greensand|12758|5|Briefly described|p22,p3 Fig. 3|Cretaceous|Cretaceous|Top part of the Coolyena Group.||||||
15386|Poison Hill Greensand|12759|4|Described|p42; p28 Tb. 7; p32 Fig 15; P36 Fig 17|||Defined Fairbridge (1953). Type section in Poison Hill, 6.5km NNW of Gingin. Max thickness is 90m.||Of Coolyena Group.||Conformably overlies the Molecap Greensand or the Gingin Chalk.|Unconsolidated pale yellow to dark green, fine- to very coarse-grained, richly glauconitic, silty and locally clayey sand.|12-MAY-14
15386|Poison Hill Greensand|14227|5|Briefly described|Enclos. 2|Late Cretaceous|Late Cretaceous|Of Coolyena Group.||||||07-FEB-11
15386|Poison Hill Greensand|23279|6|Mentioned|p31|||||||||
15386|Poison Hill Greensand|23816|4|Described|p251|Late Cretaceous|Late Cretaceous|Geological Province: Perth Basin. Uppermost unit of the Coolyena Group. Underlying unit: Gingin Chalk (conformable). Max. thickness: >45 m.||||||11-DEC-06
15386|Poison Hill Greensand|24094|5|Briefly described|Not recorded|||Geological Province: Perth Basin.||||||16-MAR-05
15386|Poison Hill Greensand|24160|6|Mentioned|p95 Tb.57.|Late Cretaceous|Late Cretaceous|||||Overlies Gingin Chalk.||
15386|Poison Hill Greensand|29693|6|Mentioned|p66|||||||||
15386|Poison Hill Greensand|30188|2|Defined|p76|Late Cretaceous|Late Cretaceous|Refers Fairbridge(1953)||||||
15386|Poison Hill Greensand|31153|6|Mentioned|Fig. 57|||Refers Cockbain & Playford (1973). Stratigraphic table.||||||
15386|Poison Hill Greensand|31238|6|Mentioned|p27|||See also Fig. 12A||||||
15386|Poison Hill Greensand|31396|6|Mentioned|p1183|||See also P1184||||||
15386|Poison Hill Greensand|31562|6|Mentioned|p11|||Stratigraphic table P10||||||
15386|Poison Hill Greensand|31912|6|Mentioned|p55|||||||||
15386|Poison Hill Greensand|32391|6|Mentioned|p1|||||||||
15386|Poison Hill Greensand|32648|6|Mentioned|p32|||U.Cret.||||||
15386|Poison Hill Greensand|33044|4|Described|p44|||See also diag. 16,21||||||
15386|Poison Hill Greensand|33165|6|Mentioned|Chart|||Correlation chart only||||||
15386|Poison Hill Greensand|34413|6|Mentioned|p13|||Senonian||||||
15386|Poison Hill Greensand|34414|6|Mentioned|p53|||||||||
15386|Poison Hill Greensand|35057|5|Briefly described|p301|||||||||
15386|Poison Hill Greensand|35282|6|Mentioned|Fig.2|||||||||
15386|Poison Hill Greensand|35638|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
15386|Poison Hill Greensand|35968|5|Briefly described|p64|||See also Table 4.||||||
15386|Poison Hill Greensand|35970|6|Mentioned|Table 12|||||||||
15386|Poison Hill Greensand|35973|5|Briefly described|p93|||||||||
15386|Poison Hill Greensand|36257|6|Mentioned|Table 2.1|||||||||
15386|Poison Hill Greensand|36265|5|Briefly described|Fig.3.26|Late Cretaceous|Late Cretaceous|Of the Coolyena Group. Geological province: Perth Basin.||||||04-MAR-08
15386|Poison Hill Greensand|36293|2|Defined|p190|Maastrichtian|Campanian|Campanian to Maastrichtian.||||||
15386|Poison Hill Greensand|36305|6|Mentioned|p353|||||||||
15386|Poison Hill Greensand|36890|3|Fully described|p250|||||||||
15386|Poison Hill Greensand|37104|6|Mentioned|Fig.3|||||||||
15386|Poison Hill Greensand|37307|5|Briefly described|p34|||||||||
15386|Poison Hill Greensand|37360|6|Mentioned|Fig.3|||||||||
15386|Poison Hill Greensand|38444|6|Mentioned|p300|||See also P301.||||||
15386|Poison Hill Greensand|39211|6|Mentioned|Fig.41|||||||||
15386|Poison Hill Greensand|40348|6|Mentioned|Map legend|Campanian|Campanian|Prob. Campanian||||||
15386|Poison Hill Greensand|40349|5|Briefly described|p17|||||||||
15386|Poison Hill Greensand|41341|6|Mentioned|p51|||||||||
15386|Poison Hill Greensand|41838|5|Briefly described|p6|||||||||
15386|Poison Hill Greensand|42123|4|Described|p21|||||||||
15386|Poison Hill Greensand|42995|5|Briefly described|Table 1|||||||||
15386|Poison Hill Greensand|43347|6|Mentioned|9|||||||||
15386|Poison Hill Greensand|43700|6|Mentioned|p25|||||||||
15386|Poison Hill Greensand|44144|4|Described|p503 Tb.4-21, p517|Maastrichtian|Campanian|Type Section: Poison Hill; 31o18'S 115o53'E.  45m thick marine shelf deposits.||Coolyena Group||Overlies Gingin Chalk conformably or Warnbro Group disconformably.|Medium- to coarse-grained greensand, and glauconitic sandstone.|
15386|Poison Hill Greensand|46883|6|Mentioned|p211|||||||||
15386|Poison Hill Greensand|61811|4|Described|p3 Fig.2, pp53-57, p65.|Campanian|Campanian|Northern Perth Basin. Type section is the ridge immediately south of 'Koorian' farmhouse off the Brand Highway, 4.2 km N of Dewar Road; further details in Appendix 1. Associated with Yallalie impact event.||Unit in Coolyena Group.||Overlies Dandaragan Sandstone and Leederville Formation. Conformably overlies Gingin Chalk.|Massive bioturbated and cross-bedded quartz and glauconite sandstone; upper part locally ferruginised sandy breccia, containing siltstone clasts from Yarragadee Formation or Parmelia Group.|
15386|Poison Hill Greensand|64580|6|Mentioned|map legend|||Of Coolyena Group.||||||15-DEC-08
15386|Poison Hill Greensand|64635|5|Briefly described|p4 Fig.3, |Campanian|Campanian|||Unit in Coolyena Group.||||
15386|Poison Hill Greensand|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||Coolyena Group.||||
15386|Poison Hill Greensand|68254|6|Mentioned|p1046 Tb.4|||||||||
15386|Poison Hill Greensand|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p55, Ch2 p57|Upper Cretaceous|Upper Cretaceous|Perth Basin.||Coolyena Group||Overlies the Gingin Chalk. Unconformably overlain by the Kings Park Shale. Is equivalent to the Lancelin Formation.||
15386|Poison Hill Greensand|69297|6|Mentioned|p175, p189|Maastrichtian|Campanian|Vlaming Sub-basin, South Perth Basin.||Coolyena Group||Overlies the Gingin Chalk. Unconformably overlain by the Kings Park Shale.||
15386|Poison Hill Greensand|70097|5|Briefly described|p20 Fig.4|Maastrichtian|Santonian|Northern Perth Basin. Dandaragan Trough.||Coolyena Group||Overlies Gingin Chalk.|Sandstone.|12-SEP-17
15386|Poison Hill Greensand|70099|5|Briefly described|Fig.4; p6|Maastrichtian|Campanian|Southern Perth Basin. Shallow marine sediments. Equivalent in age to deep marine, carbonate-dominated sedimentation of Mentelle 9 Supersequence.||Coolyena Group.||Overlies Gingin Chalk.||
15386|Poison Hill Greensand|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||claystone, greensand|
15388|Pokegama Quartzite|41997|6|Mentioned|p72|||||||||
15393|Polda Formation|23792|5|Briefly described|Fig.D4|Kimmeridgian|Callovian|Equivalent to Sea Lion supersequence. Geological Province: Bight Basin.||||||
15393|Polda Formation|24201|5|Briefly described|p373 Fig. 2|||Name used to describe unnamed equivalent of Polda Formation.||||||
15393|Polda Formation|24338|5|Briefly described|p938 Fig. 2|Kimmeridgian|Callovian|Overlain by the Echidna Formation. Formation is Fm in text. Geological Province: Bight Basin. Is unnamed in text but is referred to as the Polda Formation Equivalent.||||||
15393|Polda Formation|24350|5|Briefly described|Fig. 4 Appdx|Late Jurassic|Middle Jurassic|Mentioned only in terms of an unnamed equivalent, in the Sea Lion Supersequence.||||||
15393|Polda Formation|24443|6|Mentioned|Fig.7|||Used as Polda Formation equivalent.||||||
15393|Polda Formation|24553|5|Briefly described|p36|Jurassic|Jurassic|Geological Province: Polda Trough.||||||07-FEB-11
15393|Polda Formation|29856|6|Mentioned|p37|||||||||
15393|Polda Formation|35672|6|Mentioned|p11|||||||||
15393|Polda Formation|37850|2|Defined|p13|Late Jurassic|Late Jurassic|||||||
15393|Polda Formation|37851|6|Mentioned|p10|||||||||
15393|Polda Formation|39211|6|Mentioned|Fig.42|||||||||
15393|Polda Formation|40445|6|Mentioned|p52|||||||||
15393|Polda Formation|40448|4|Described|p41|||||||||
15393|Polda Formation|40673|6|Mentioned|p11|||||||||
15393|Polda Formation|41218|6|Mentioned|p328|||||||||
15393|Polda Formation|41363|6|Mentioned|p16|||||||||
15393|Polda Formation|42648|5|Briefly described|p48|||||||||
15393|Polda Formation|42716|5|Briefly described|Map legend|Jurassic||||||||
15393|Polda Formation|42738|5|Briefly described|map legend|Jurassic||||||||
15393|Polda Formation|43026|5|Briefly described|Table 5,p591|||||||||
15393|Polda Formation|43049|4|Described|p21|||||||||
15393|Polda Formation|43052|5|Briefly described|Table 2.1|||||||||
15393|Polda Formation|43053|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||25-MAY-05
15393|Polda Formation|43258|5|Briefly described|Map Legend||Jurassic|||||||
15393|Polda Formation|43298|5|Briefly described|Map Legend||Jurassic|||||||
15393|Polda Formation|44133|4|Described|p72 Fig. 8.11, 131|Late Jurassic|Middle Jurassic|Geological Province: Polda Basin. Overlies Kilroo Formation. Unconformably overlies: Coolardie Formation. Disconformably overlain by the Poelpena Formation. Type section ~86m thick.||||||11-JUL-13
15393|Polda Formation|44145|6|Mentioned|p549  |||South Australian rocks broadly similar to Loongana Formation.||||||
15393|Polda Formation|60953|5|Briefly described|Map Legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||
15393|Polda Formation|61108|5|Briefly described|map legend|Jurassic|Jurassic|Fluvial sandstone and conglomerate.||||||
15393|Polda Formation|61544|6|Mentioned|p367 Fig.3. |||Is equivalent to the unit underlying Echidna Formation in the Ceduna Sub-basin.||||||
15393|Polda Formation|62893|4|Described|Map Legend, p18-20, p22, p29|Late Jurassic|Late Jurassic|Polda Basin (only). Fluviatile to lacustrine sequence. Type section is in SADME Polda 1 drillhole where it is 86 m thick. Thickness ranges from 11 m to 282 m. Three informal members were described by Gatehouse and Cooper (1982) from the type section, although the sections change greatly between holes. Correlates with the Late Jurassic J6 microflora of Evans (1966). Overlies Archaean-Proterozoic basement rocks on the southern basin margin.||||Unconformably underlain by Coolardie Formation. Disconformably overlain by Poelpena Formation.|Grey, brown and black clayey sand, grey to dark grey carbonaceous silt, and clay beds with interlayered lignite and coal and also quartz and kaolin-rich cobbly conglomerate.|
15393|Polda Formation|65376|6|Mentioned|p38, p41.|Jurassic|Jurassic|||||||
15393|Polda Formation|68135|5|Briefly described|p52 fig 2b |Oxfordian|Callovian||||||Interbedded siltstone and sandstone.|14-SEP-17
15393|Polda Formation|69297|6|Mentioned|p58|Early Cretaceous|Middle Jurassic|||||||
15393|Polda Formation|71037|6|Mentioned|p21 Fig.1|Jurassic|Jurassic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as younger than Tent Hill Formation and older than unnamed undifferentiated Tertiary sediments.||
15393|Polda Formation|71559|6|Mentioned|p15 Fig 1|Jurassic|Jurassic|Geological province: Gawler Craton.||||||
15393|Polda Formation|71859|6|Mentioned|p6, p18|Jurassic|Jurassic|||||||
15393|Polda Formation|73130|6|Mentioned|[poster] Fig.1|Jurassic|Jurassic|||||||28-OCT-22
15411|Pollock Hills Formation|24197|5|Briefly described|p141, p143|||Comagmatic felsic volcanics with Mount Webb Granite. See also the misspelt Polloch Hills Formation. See p143, p146 for lithological detail.||||||07-FEB-11
15411|Pollock Hills Formation|29806|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|29807|4|Described|Table 1|||||||||
15411|Pollock Hills Formation|35201|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|35223|4|Described|Table.2|||||||||
15411|Pollock Hills Formation|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15411|Pollock Hills Formation|37299|6|Mentioned|Fig.1|||||||||
15411|Pollock Hills Formation|39887|6|Mentioned|p452|||||||||
15411|Pollock Hills Formation|39888|6|Mentioned|Fig.9|||||||||
15411|Pollock Hills Formation|42504|5|Briefly described|Table 3 P60|||||||||
15411|Pollock Hills Formation|44194|4|Described|p3|Proterozoic|Proterozoic|Felsic volcanics co-magmatic with Mount Webb Granite. SHRIMP dating done but no satisfactory igneous crystallisation age obtained.||||||
15411|Pollock Hills Formation|45140|2|Defined|p12-13, p26, p28-34, p36-38, p60, p74|Calymmian|Calymmian|See also Appx.p14-15. New name: Blake (1977). Arunta Block. Named after the Pollock Hills, in which is the type section, from 22deg 50'S, 127deg 40'E to 22deg 49'S, 127deg 38'E. Over 1000m thick. Lithologies detailed. A preferred age given is 1526 +/- 25 Ma (Page et al., 1976). Geochemistry detailed.|1510+/-240 Ma (Rb-Sr whole-rock: Page et al.1976)|||Unconformably overlies Arunta Complex. Is intruded by (and probably co-magmatic with) Mount Webb Granite. Is overlain unconformably by Heavitree Quartzite.|Unmetamorphosed acid lavas and associated sedimentary rocks. At the type section, porphyritic acid lava (unknown thickness) is overlain by 600m of interbedded, medium- to thin-bedded lithic arenite, sublithic arenite and tuffaceous sandstone.|
15411|Pollock Hills Formation|46788|4|Described|p6|||||||||
15411|Pollock Hills Formation|50369|5|Briefly described|p1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Mount Webb Suite. Age: ignimbrite 1643 +/- 13, Ma, SHRIMP, 1478 +/- 240Ma Rb/Sr.||||||28-SEP-12
15411|Pollock Hills Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Dacite, rhyodacite, and volcaniclastic sedimentary rock.||||||09-DEC-08
15411|Pollock Hills Formation|65074|4|Described|p349-350, p352-353, p354 Tb.4-11, p360|Mesoproterozoic|Mesoproterozoic|See also p362. Of SW Birrindudu Basin. Type locality is in the Pollock Hills: details given. 1-1.5 km thick. Lava units are probably comagmatic with Mount Webb Granite. Whole-rock Rb-Sr dating of acid lavas. An Rb-Sr isochron age is also given of 1526 +/- 25 Ma.|1510 +/- 240 Ma (Page et al., 1976).|||Intruded by Mount Webb Granite. Is overlain unconformably by Heavitree Quartzite.|Dacitic lavas and tuffs, arenite, tuffaceous sandstone, conglomerate, lapilli tuff, agglomerate.|
15411|Pollock Hills Formation|68994|4|Described|p1, p4-11, p16, p23-27|Statherian|Statherian|Warumpi Province. Magmatic crytallisation age of dacite. Detrital zircon U-Pb ages listed and Hf analyses detailed (Wingate et al. 2012). Volcanic age based on single youngest zircon analysis, 1643+/-13 Ma (Wyborn et al. 1998).|1677+/-6 Ma.|||Is overlain unconformably by Kiwirrkurra Formation.|Consists mainly of altered, black porphyritic metadacite and metarhyodacite, overlain by volcaniclastic sedimentary rocks.|13-JAN-17
15411|Pollock Hills Formation|69003|5|Briefly described|p5, p32|Paleoproterozoic|Paleoproterozoic|West Arunta Orogen.|c.1670 Ma.|||Overlies Ininti Granite.|Volcaniclastic rocks.|
15411|Pollock Hills Formation|69031|5|Briefly described|p4, p7-8, p15|Statherian|Statherian|Warumpi Province, Arunta Orogen. Previously thought to be coeval with Mount Webb Granite; geochronology establishes a c.30 m.y. separation. Source of sediment for Kiwirrkura Formation. Magnetic susceptibility data.|c.1670 Ma (U-Pb zircon: Wingate, 2012).|||Is intruded by Ininti Granite.|Includes chert, tuff, lavas including rhyodacite.|
15411|Pollock Hills Formation|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Metadacite, metarhyodacite, and volcaniclastic metasedimentary rock.|
15411|Pollock Hills Formation|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
15411|Pollock Hills Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, ash tuff, agglomerate, sandstone|
15411|Pollock Hills Formation|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|||||Ignimbrite.|
15411|Pollock Hills Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|1677+/-6 Ma||||Metadacite, metarhyodacite, and volcaniclastic metasedimentary rock.|
15445|Poondano Formation|22717|5|Briefly described|P13||Tertiary|||||||
15445|Poondano Formation|24573|6|Mentioned|p671|||Geological Province: Pilbara Craton and minor deposits of the Yilgarn Craton||||||
15445|Poondano Formation|32648|6|Mentioned|p32|||Pliocene||||||
15445|Poondano Formation|36890|4|Described|p356|||||||||
15445|Poondano Formation|37564|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15445|Poondano Formation|37633|5|Briefly described|p13|||||||||
15445|Poondano Formation|38878|6|Mentioned|Map legend|Miocene|Miocene|||||||
15445|Poondano Formation|39426|6|Mentioned|p15|||||||||
15445|Poondano Formation|39697|6|Mentioned|p138|||||||||
15445|Poondano Formation|41271|6|Mentioned|p175|||||||||
15445|Poondano Formation|44478|14|Not recorded|map legend||Tertiary|||||||
15445|Poondano Formation|44501|6|Mentioned|table 7, map||Tertiary|(mis-spelt Poondana Formation in table1.p.7). (F/50-7).||||||
15445|Poondano Formation|44502|14|Not recorded|map legend||Tertiary|||||||
15445|Poondano Formation|44536|14|Not recorded|map legend|||Correlation||||||
15445|Poondano Formation|44998|2|Defined|p189||Jurassic|Overlies Precambrian crystalline rocks. On many pages. p120,190-4,249, map.||||||16-JAN-12
15445|Poondano Formation|45158|3|Fully described|p10|||See also P34||||||
15445|Poondano Formation|50189|6|Mentioned|p29|Cenozoic|Cenozoic|Originally described in the Port Headland area.||||||19-NOV-08
15445|Poondano Formation|61155|5|Briefly described|p16|Late Eocene|Late Eocene|Age: ~40.5-36.5Ma. Thickness: 8m. Geological Province: Southern Canning Basin.||||||
15445|Poondano Formation|63236|5|Briefly described|map legend|Cenozoic|Cenozoic|Channel iron deposits and pisolite - pisolitic and limonitic riverine palaeochannel mineralisation.||||||17-SEP-07
15445|Poondano Formation|63432|5|Briefly described|p734|||Geological Province: Pilbara Province. Channel iron deposit.||||||07-FEB-11
15445|Poondano Formation|64688|5|Briefly described|Map legend|||Channel iron deposits and pisolite.||||||
15445|Poondano Formation|65008|6|Mentioned|p25|||||||||
15445|Poondano Formation|70826|6|Mentioned|p7 tbl 4|Miocene|Eocene|Pilbara region.||||||30-APR-20
15445|Poondano Formation|72447|6|Mentioned|p237-240|||Pilbara Craton. Hosts fossiliferous iron-rich pisolitic deposits (channel iron deposits).||||Equivalent to Robe Pisolite Formation.||
15517|Poulton Formation|7433|5|Briefly described|p25 Fig.2, p29, p30 Fig.6. |Early Devonian|Early Devonian|Canning Basin; Lennard Shelf. Fine marine clastics.||||Inferred to partly grade into Tandalgoo Sandstone.||
15517|Poulton Formation|13255|6|Mentioned|p368|Middle Devonian|Early Devonian|Oobagooma Sub-basin, Roebuck Basin.||||Is ovelain by Pillara Reef Complex.||
15517|Poulton Formation|14228|6|Mentioned|p6 fig3|Givetian|Givetian|North Canning Basin.||||||
15517|Poulton Formation|22718|6|Mentioned|P4|||||||||
15517|Poulton Formation|22741|6|Mentioned|P24||Devonian|||||||
15517|Poulton Formation|22753|5|Briefly described|Fig.3 p585|Devonian|Devonian|||||||
15517|Poulton Formation|22764|4|Described|Table2,p11|Middle Devonian|Early Devonian|?100.||||||01-FEB-10
15517|Poulton Formation|22776|3|Fully described|p17, Table.3|Middle Devonian|Middle Devonian|Confined to Lennard Shelf.||||||
15517|Poulton Formation|22814|5|Briefly described|fig2|Devonian|Devonian|||||||
15517|Poulton Formation|24061|5|Briefly described|p178|Middle Devonian|Middle Devonian|Geological Province: Canning Basin.||||||10-NOV-08
15517|Poulton Formation|29813|6|Mentioned|p16|||||||||
15517|Poulton Formation|30595|5|Briefly described|p3|||||||||
15517|Poulton Formation|32648|6|Mentioned|p32|||L.-mid Dev.||||||
15517|Poulton Formation|33518|6|Mentioned|p8|||||||||
15517|Poulton Formation|33965|6|Mentioned|p12|||||||||
15517|Poulton Formation|35119|6|Mentioned|p462|Middle Devonian|Middle Devonian|Overlies Nita Formation in Blackstone No. 1.||||||21-APR-17
15517|Poulton Formation|35120|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Prob.E - M Devonian E - M||||||
15517|Poulton Formation|36224|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|Siltstone, minor shale, sandstone; traces of dolomite.||||||01-FEB-05
15517|Poulton Formation|36257|6|Mentioned|Table 2.1|||||||||
15517|Poulton Formation|36890|3|Fully described|p328|||Formerly Blackstone Formation.||||||
15517|Poulton Formation|38878|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early Devonian - Middle DevonianE - M||||||
15517|Poulton Formation|40837|6|Mentioned|p260|||||||||
15517|Poulton Formation|41023|6|Mentioned|Fig.3|||||||||
15517|Poulton Formation|41169|6|Mentioned|p141|||See also Fig.3||||||
15517|Poulton Formation|41215|6|Mentioned|p267|||||||||
15517|Poulton Formation|42030|4|Described|p747|||||||||
15517|Poulton Formation|42338|5|Briefly described|Table 1 P145|||||||||
15517|Poulton Formation|42347|6|Mentioned|Fig.2 p1020|||||||||25-FEB-20
15517|Poulton Formation|42792|5|Briefly described|Table 1 P225|||||||||
15517|Poulton Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
15517|Poulton Formation|42930|5|Briefly described|Fig.1 p473|Devonian|Devonian|Overlies and interfingers with Tandalgoo Red Beds; partly underlies and interfingers with Mellinjerie Limestone. Geological Province: Canning Basin.||||||13-NOV-07
15517|Poulton Formation|42933|5|Briefly described|Fig.94 p258|||||||||
15517|Poulton Formation|43173|5|Briefly described|54||Middle Devonian|||||||
15517|Poulton Formation|43563|6|Mentioned|Fig.2,p6|||||||||
15517|Poulton Formation|43599|6|Mentioned|p250, Fig.3|||||||||
15517|Poulton Formation|43656|6|Mentioned|Fig.2,p8|Givetian|Eifelian|||||||
15517|Poulton Formation|43666|6|Mentioned|p16|||||||||
15517|Poulton Formation|43746|6|Mentioned|Fig.2,p11|Givetian|Eifelian|||||||
15517|Poulton Formation|43803|3|Fully described|p69-70||Devonian|||||||
15517|Poulton Formation|43815|6|Mentioned|p93|||||||||
15517|Poulton Formation|43818|6|Mentioned|Fig.2.p39|Middle Devonian|Early Devonian|||||||
15517|Poulton Formation|43932|6|Mentioned|p4|||||||||
15517|Poulton Formation|44143|4|Described|p439 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 400m thick; red-brown to red siltstone; shallow marine. Type section between 1,941 and 2,220 m in Blackstone 1 (DERBY: 17deg 35' 14" S, 124deg 21' 01" E).||||||24-NOV-17
15517|Poulton Formation|45153|2|Defined|App.2-27|Middle Devonian|Middle Devonian|||||||
15517|Poulton Formation|45158|3|Fully described|p26|||||||||
15517|Poulton Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
15517|Poulton Formation|50089|5|Briefly described|p428 Fig. 2|||||||||
15517|Poulton Formation|61021|5|Briefly described|p37|Middle Devonian|Early Devonian|Geological Province: Canning Basin.||||||17-DEC-07
15517|Poulton Formation|63938|4|Described|p50|Middle Devonian|Middle Devonian|Silty red beds ~300m thick in subsurface NW Lennard Shelf. Probably older than Cadjebut Formation. Name should not be used in Prices Hill area.||||||
15517|Poulton Formation|64187|5|Briefly described|p320 Fig. 2|Middle Devonian|Middle Devonian|Formation is Fm in text. Underlain unconformably by Carribuddy Formation, overlain by Pillara Limestone. Sandstone, siltstone, shale (marine). Geological Province: Canning Basin.||||||27-JAN-10
15517|Poulton Formation|64643|4|Described|p3 Fig. 2, p35|Middle Devonian|Middle Devonian|Silty red beds ~300m thick in subsurface NW Lennard Shelf. Probably older than Cadjebut Formation. Name should not be used in Prices Hill area.||||||
15517|Poulton Formation|65214|6|Mentioned|p277|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
15517|Poulton Formation|65301|5|Briefly described|p5 Fig. 4|Middle Devonian|Middle Devonian|Geological province: Canning Basin.||||||
15517|Poulton Formation|65449|6|Mentioned|p5-6, p9, p31|Middle Devonian|Middle Devonian|Lennard Shelf.||Included in Tanndulla Group by Lehmann (1984)..||Lateral equivalent of Tandalgoo Formation.||08-APR-20
15517|Poulton Formation|66127|5|Briefly described|Plates 1, 2.|Givetian|Givetian||||||Sandstone, shale and siltstone; minor dolomite; marine.|
15517|Poulton Formation|68007|6|Mentioned|p4|Middle Devonian|Middle Devonian|Canning Basin.||||||25-FEB-20
15517|Poulton Formation|68902|6|Mentioned|p9 fig 5|Devonian|Devonian|Is overlain by (mainly Upper) Devonian reef complexes.||||||
15517|Poulton Formation|69312|6|Mentioned|p19|Devonian|Devonian|Canning Basin.||||Overlies the Tandalgoo Sandstone. Overlain by the Windjana Limestone.||
15517|Poulton Formation|69883|5|Briefly described|p21, Plate 3|Devonian|Devonian|Stratotype Intersected in Blackstone 1. Age inferred.||||Unconformably overlies the Nita Formation.||27-FEB-20
15517|Poulton Formation|70774|5|Briefly described|p4|Middle Devonian|Middle Devonian|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Equivalent to the Tandalgoo Formation.||
15517|Poulton Formation|72497|5|Briefly described|p3 Fig.2.|Givetian|Eifelian|Canning Basin. Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Unconformably underlies Babrongan Reef Complex and laterally equivalent to upper Worral Formation.||
15529|Powereena Dyke|30766|6|Mentioned|p9|||||||||
15529|Powereena Dyke|43037|6|Mentioned|Fig.6,p30|||||||||
15551|Pretlove Sandstone|13194|4|Described|p394 Tb. 4-16, p399 fig 4-63|Late Cambrian|Late Cambrian|Type Section: 6.4km SE of Clark Jump Up 15o29'S 128o40'E. 24-125m thick intertidal to shallow marine deposits.  Absent in Bonaparte Basin outliers.||Carlton Group||Overlies Skewthorpe Formation or Hart Spring Sandstone (both conformably). Part equivalent to Clark Sandstone and Skewthorpe Formation.|Quartz sandstone and siltstone.|
15551|Pretlove Sandstone|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlies Skewthorpe Formation. Overlain by Clark Sandstone.||06-OCT-16
15551|Pretlove Sandstone|24390|5|Briefly described|p2 Fig. 2||Cambrian|Geological Province: Bonaparte Basin.  Of the Carlton Group.||||||
15551|Pretlove Sandstone|31572|6|Mentioned|Fig.|||U.Cambrian. Correlation chart 1.||||||
15551|Pretlove Sandstone|32648|6|Mentioned|p32|||U.Camb.||||||
15551|Pretlove Sandstone|32664|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|Briefly described in notes||||||
15551|Pretlove Sandstone|32870|5|Briefly described|p39|||See also Fig.6||||||
15551|Pretlove Sandstone|36551|6|Mentioned|Table 16|||||||||
15551|Pretlove Sandstone|36890|3|Fully described|p375|||||||||
15551|Pretlove Sandstone|40993|6|Mentioned|p2|||||||||
15551|Pretlove Sandstone|41459|6|Mentioned|Fig.2|||||||||
15551|Pretlove Sandstone|41690|6|Mentioned|Fig.2|||||||||
15551|Pretlove Sandstone|41731|6|Mentioned|Fig.3|||||||||
15551|Pretlove Sandstone|41864|3|Fully described|p42|||||||||
15551|Pretlove Sandstone|41865|5|Briefly described|Map Legend|Late Cambrian||||||||
15551|Pretlove Sandstone|43661|6|Mentioned|Fig.3|||||||||
15551|Pretlove Sandstone|45038|14|Not recorded|Fig. 21,22,23,36||Cambrian|||||||
15551|Pretlove Sandstone|45039|6|Mentioned|Fig.2|||Upper Cambrian||||||
15551|Pretlove Sandstone|45058|6|Mentioned|Fig. 3|||See also Fig. 4. U.Cambrian||||||
15551|Pretlove Sandstone|45130|6|Mentioned|p15|||||||||
15551|Pretlove Sandstone|48886|4|Described|p.46||Late Cambrian|See also map. Upper Cambrian.||||||
15551|Pretlove Sandstone|49637|5|Briefly described|Fig. 6|Late Cambrian|Middle Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||07-FEB-11
15551|Pretlove Sandstone|50085|5|Briefly described|p2 Fig. 2|Late Cambrian|Late Cambrian|Of the Carlton Group.  Geological Province: Bonaparte Basin.||||||
15551|Pretlove Sandstone|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||10-APR-08
15551|Pretlove Sandstone|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
15551|Pretlove Sandstone|69099|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||04-AUG-15
15551|Pretlove Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
15551|Pretlove Sandstone|69437|5|Briefly described|p22:10|Series 4|Series 3|Bonaparte Basin, Centralian B Superbasin.||Carlton Group.||Overlies Skewthorpe Formation. Is overlain by Clark Sandstone.||12-JUL-16
15551|Pretlove Sandstone|69443|6|Mentioned|p28:21|||Bonaparte Basin.||||Correlated with Barkly Group.||12-JUL-16
15551|Pretlove Sandstone|69452|5|Briefly described|p36:5|Series 4|Series 3|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Conformably overlies Skewthorpe Formation. Is overlain conformably by Clark Sandstone.||12-JUL-16
15551|Pretlove Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
15551|Pretlove Sandstone|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian|||Carlton Group||Overlies Skewthorpe Formation, overlain by Clark Sandstone||
15551|Pretlove Sandstone|71146|5|Briefly described|p6|Cambrian|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Skewthorpe Formation. Overlain by the Clark Sandstone.|Sandstone.|
15573|Prices Creek Group|7433|5|Briefly described|p25 Fig.2, p28 Fig.5, p29. |Ordovician|Ordovician|Canning Basin. Marine carbonates.||||Grades laterally into Carranya beds.|Shallow marine, fine clastic and carbonate deposits.|
15573|Prices Creek Group|22741|5|Briefly described|P21, Table3 P18||Ordovician|||||||
15573|Prices Creek Group|23903|5|Briefly described|p1597 Fig.2|Ordovician|Ordovician|Geological Province: Canning Basin.||||||27-NOV-06
15573|Prices Creek Group|30983|4|Described|p73|||||||||
15573|Prices Creek Group|31870|6|Mentioned|p8|||||||||
15573|Prices Creek Group|32648|6|Mentioned|p32|||Camb.-Ord.||||||
15573|Prices Creek Group|32979|6|Mentioned|p38|||Correlation with basins in India.||||||
15573|Prices Creek Group|35104|6|Mentioned|Fig.2|||||||||
15573|Prices Creek Group|35119|4|Described|p460|||See also p448.||||||27-NOV-06
15573|Prices Creek Group|36225|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15573|Prices Creek Group|36890|6|Mentioned|p321|||||||||
15573|Prices Creek Group|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
15573|Prices Creek Group|40136|5|Briefly described|p37|||||||||
15573|Prices Creek Group|40810|5|Briefly described|p14|||||||||
15573|Prices Creek Group|41854|6|Mentioned|p94|||||||||
15573|Prices Creek Group|41894|6|Mentioned|p2|||||||||
15573|Prices Creek Group|43563|6|Mentioned|p4|Early Ordovician|Early Ordovician|(E.Ord-M.Ord)||||||
15573|Prices Creek Group|43803|6|Mentioned|p65||Ordovician|||||||
15573|Prices Creek Group|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
15573|Prices Creek Group|43819|6|Mentioned|p31||Arenig|||||||
15573|Prices Creek Group|43876|14|Not recorded|p553||Ordian|||||||
15573|Prices Creek Group|44143|6|Mentioned|p.426, p441 Tb. 4-19|Ordovician|Ordovician|Lennard Shelf. Includes Gap Creek and Emanuel Formations. Shallow marine carbonates and siliciclastics. Correlated with Nambeet and Willara Formations.||||||
15573|Prices Creek Group|44309|14|Not recorded|p12|||Fauna correlated with Coolibah Formation.||||||
15573|Prices Creek Group|44397|14|Not recorded|p.12|||||||||
15573|Prices Creek Group|44403|6|Mentioned|p.8||Ordovician|||||||
15573|Prices Creek Group|44404|14|Not recorded|map legend||Ordovician|||||||
15573|Prices Creek Group|44998|2|Defined|p18, map.|||||||||
15573|Prices Creek Group|45153|6|Mentioned|App.1-14|||||||||
15573|Prices Creek Group|45158|3|Fully described|p28|||||||||
15573|Prices Creek Group|48826|14|Not recorded|Tb.III|||||||||
15573|Prices Creek Group|48874|14|Not recorded|p.3|||||||||
15573|Prices Creek Group|63938|4|Described|p48, p52 Fig.4|Middle Ordovician|Early Ordovician|Unconformably overlain by Cadjebut Formation in the Emanuel Range.||||||10-NOV-08
15573|Prices Creek Group|64334|5|Briefly described|p39-40|Ordovician|Ordovician|Eastern Lennard Shelf, Canning Basin. Tremadoc-Arenig.|||Gap Creek, Emanuel Formations; Kudata Dolomite; Kunian Sandstone.|Correlates with Nambeet and Willara Formations.||
15573|Prices Creek Group|64502|5|Briefly described|p765 Fig.2, p768 Fig.5|Ordovician||||||||
15573|Prices Creek Group|64580|4|Described|map legend|Middle Ordovician|Early Ordovician|Siltstone, shale, limestone, and dolomitic sandstone; includes KUNIAN SANDSTONE, KUDATA DOLOMITE, EMANUEL and GAP CREEK FORMATIONS.||||||09-DEC-08
15573|Prices Creek Group|64643|4|Described|p3 Fig. 2, p33, 37|Middle Ordovician|Lower Ordovician|||||||
15573|Prices Creek Group|65301|5|Briefly described|p5 Fig. 4|Middle Ordovician|Early Ordovician|Geological province: Canning Basin.||||||
15573|Prices Creek Group|65449|6|Mentioned|p6|Middle Ordovician|Early Ordovician|||||||
15573|Prices Creek Group|65486|5|Briefly described|p6-7,9,17; Figs.5,67,19; Plate 1.|Ordovician|Ordovician|Dolomite, shale, and siltstone, Canning Basin. Unconformably underlies Pillara Limestone, Cadjebut Formation, Carolyn Formation (Grant Group).||||||
15573|Prices Creek Group|66127|5|Briefly described|pp19-21, p24, p68, Plates 4,5,7,8.|Middle Ordovician|Early Ordovician|Unconformably overlies Proterozoic rocks.|||Includes Emanuel and Gap Creek Formations.|Unconformably underlies Cadjebut Formation.|Dolomite, shale and siltstone.|
15573|Prices Creek Group|68007|6|Mentioned|p4|Ordovician|Ordovician|Canning Basin.||||||
15573|Prices Creek Group|68902|6|Mentioned|p9 fig 5|Ordovician|Ordovician||||Includes Carranya Formation|||
15573|Prices Creek Group|69099|4|Described|500k_geologyp08_lut.csv|Middle Ordovician|Early Ordovician||||Includes Kunian Sandstone, Kudata Dolomite, Emanuel and Gap Creek Formations||Siltstone, shale, limestone, and dolomitic sandstone.|04-AUG-15
15573|Prices Creek Group|69165|4|Described|500k_geologyp08_lut.csv|Ordovician|Ordovician||||Includes Kunian Sandstone, Kudata Dolomite, Emanuel Formation, Gap Creek Formation||Undivided; siltstone, shale, limestone and dolomitic sandstone|
15573|Prices Creek Group|69182|6|Mentioned|Ch4 p9-p12, Ch4 p40-p41|||Canning Basin. See also Ch4 p45,Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92, Ch4 p94.||||||
15573|Prices Creek Group|69883|5|Briefly described|p4-p5|Arenig|Tremadocian|Canning Basin. Conodont zones and supersequences provided.|||Includes the Kunian Sandstone, Kudata Dolomite, Emanuel Formation and Gap Creek Formation.|||
15573|Prices Creek Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Middle Ordovician|Lower Ordovician||458-485 Ma||||Siltstone, shale, limestone, and dolomitic sandstone|
15573|Prices Creek Group|70774|5|Briefly described|p4|Middle Ordovician|Early Ordovician|Fitzroy Trough and Lennard Shelf, Canning Basin.||||||06-FEB-20
15573|Prices Creek Group|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Canning Basin.||||||
15573|Prices Creek Group|71146|6|Mentioned|p24, p26|||Canning Basin.|||Includes the Kudata Dolomite and the Kunian Sandstone.|||
15573|Prices Creek Group|71171|5|Briefly described|p1-p2, p4|||Canning Basin.|||Includes the Kunian Sandstone, Carranya Formation, Kudata Dolomite, Emanuel Formation, Gap Creek Formation, Nambeet Formation and Willara Formation.|||
15573|Prices Creek Group|71267|4|Described|GEOL_LUT_CSV files|Middle Ordovician|Early Ordovician|Of Canning Basin. Events: Point Moody Extension (300-242 Ma); Red Bluffs Extension (372.2-360 Ma); Van Emmerick Extension (382.7-372.2 Ma); Samphire Marsh Extension (485-480 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|485.4-458.4 Ma (bistrat)||Includes Emanuel Formation, Gap Creek Formation.||Siltstone, shale, limestone, and dolomitic sandstone|
15573|Prices Creek Group|71870|5|Briefly described|p5|||Canning Basin.||||Equivalent to the Nambeet Formation.||
15573|Prices Creek Group|71894|5|Briefly described|p4|Lower Ordovician|Lower Ordovician|Canning Basin.||||Overlies the Carranya Formation.|Cabonate and shale.|
15573|Prices Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Middle Ordovician|Early Ordovician|Canning Basin.  Age from biostratigraphy.|||||Siltstone, shale, limestone, and dolomitic sandstone.|
15573|Prices Creek Group|72499|5|Briefly described|p7 Fig.6.|Middle Ordovician|Early Ordovician|Located in the Fitzroy Trough.||||Overlies Carranya Formation.|Includes carbonate shales.|
15573|Prices Creek Group|72503|6|Mentioned|p26|||Canning Basin. Crops out along the Lennard Shelf.||||||
15573|Prices Creek Group|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[?] Carranya Formation.|Dominantly carbonate-shale, marl.|
15573|Prices Creek Group|73344|5|Briefly described|p2-4, p6, p41, p50-51, p53, p56, p62-65|Middle Ordovician|Early Ordovician|Canning Basin, Lennard Shelf. Known from the subsurface and outcrops. Part of supersequence A.|||Gap Creek Formation, Emanuel Formation, Kudata Dolomite, Kunian Sandstone|Equivalent to Nambeet Formation and Willara Formation.||07-DEC-22
15573|Prices Creek Group|73346|6|Mentioned|p1-3|Ordovician|Ordovician|Canning Basin, Lennard Shelf. Outcrops in the Emanuel Range as a small inlier.||||||
15573|Prices Creek Group|73567|6|Mentioned|p62|Ordovician|Ordovician|Canning Basin, Lennard Shelf.|||Emanuel Formation, Gap Creek Formation|Equivalent to the Nambeet and Willara formations.||
15592|Prince of Wales Granodiorite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Foliated and recrystalised hornblende-biotite granodiorite.|
15592|Prince of Wales Granodiorite|41914|4|Described|p21|||||||||
15592|Prince of Wales Granodiorite|68066|5|Briefly described|p5 Fig. 2, p27, map|Archean|Archean|Small (10 x 2 km) poorly exposed body of granitoid.|||||Coarse-grained, strongly foliated, hornblende-biotite granodiorite with evidence of a complex recrystallization history.|
15604|Prion 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
15604|Prion Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Paleogene|Browse Basin.||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Palaeogene|Unit of Woodbine Group. Overlies Bassett Formation and underlies Cartier Formation.||83||||28-OCT-14
15604|Prion Formation|22663|5|Briefly described|AC97 1-4 Fig.4|Oligocene|Eocene|Of the Woodbine Group.||||||01-MAR-10
15604|Prion Formation|23378|6|Mentioned|p180 Fig.2||Eocene|Of the Woodbine Group. In the Vulcan Sub-basin.||||||27-NOV-06
15604|Prion Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province: Vulcan Sub-Basin.||||||20-SEP-14
15604|Prion Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
15604|Prion Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
15604|Prion Formation|42066|5|Briefly described|Fig.3 P199|||||||||
15604|Prion Formation|60634|6|Mentioned|p1168 Fig.3. |Oligocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation. Is overlain by Oliver Formation.||
15604|Prion Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
15604|Prion Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation.||
15604|Prion Formation|62837|5|Briefly described|Stratigraphic columns|Oligocene|Eocene|Age: ~41-~33Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
15604|Prion Formation|63358|5|Briefly described|p4 Fig. 1.3|Oligocene|Eocene|||||||01-MAR-10
15604|Prion Formation|64695|5|Briefly described|p260, p262|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Hibernia Formation. Is overlain unconformably by Oliver Formation.||
15604|Prion Formation|66187|5|Briefly described|p413 Fig.2|Eocene||Unit in the Woodbine Group. Underlies the Oliver Formation unconformably; overlies the Hibernia Formation. Mount Ashmore Dome.||||||
15604|Prion Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
15604|Prion Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
15604|Prion Formation|69673|6|Mentioned|p174|||||||||
15604|Prion Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.||Overlies Hibernia Formation. Is overlain by Cartier Formation.||12-JUL-16
15624|Prospect Shale|29845|6|Mentioned|p196|||||||||
15632|Prudhoe Formation|42053|4|Described|p45|||||||||01-MAR-10
15637|Pteropus Breccia|41158|6|Mentioned|Table 13|||||||||
15646|Puffin Formation|5952|5|Briefly described|p215 Fig. 5, p223|Late Cretaceous|Late Cretaceous|Appears as Puffin in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
15646|Puffin Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||Is overlain by Bassett Formation.||
15646|Puffin Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cretaceous|Cretaceous|Type section Grebe 1 well (2098-2630m). Up to 570m thick. Oil reservoir on Ashmore Platform.||Bathurst Island Group||Overlies Vee Formation (conformably but diachronous). Grades into Turnstone Formation and Brown Gannet Limestone.|Sandstone interbedded with lesser shale and marl. Petroleum.|
15646|Puffin Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||Is overlain by Bassett Formation.||
15646|Puffin Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Fenelon and Gibson Formations, and underlies Bassett Formation of the Woodbine Group.||125||||28-OCT-14
15646|Puffin Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Cretaceous|Of the Bathurst Island Group.||||||01-MAR-10
15646|Puffin Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||27-NOV-06
15646|Puffin Formation|23378|5|Briefly described|p180 Fig.2||Cretaceous|Of the Bathurst Island Group. In the Vulcan Sub-basin.||||||01-MAR-10
15646|Puffin Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
15646|Puffin Formation|24207|6|Mentioned|p210 Fig. 6|||Referred to as Puffin only in Figure 6.||||||
15646|Puffin Formation|41459|6|Mentioned|Fig.2|||Reserved as Puffin.||||||27-NOV-06
15646|Puffin Formation|41532|2|Defined|p308|Late Cretaceous||||||||
15646|Puffin Formation|41731|6|Mentioned|Fig.3|||||||||
15646|Puffin Formation|42053|4|Described|p45|||See also Fig. 2 p29.||||||01-MAR-10
15646|Puffin Formation|42066|5|Briefly described|Fig.3 P199|||||||||
15646|Puffin Formation|42442|3|Fully described|p29|Danian|Campanian|Age: Late Cretaceous to early Paleocene. Type section in Grebe 1 between 2125 and 2630 m. Restricted to eastern Ashmore Platform and Vulcan Sub-basin. Max thickness 570 m.|||||lenticular sandstones interbedded with shale|01-NOV-12
15646|Puffin Formation|42861|6|Mentioned|p4|||||||||
15646|Puffin Formation|43661|6|Mentioned|Fig.3|||||||||
15646|Puffin Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
15646|Puffin Formation|43739|6|Mentioned|Fig.5,p38|||||||||
15646|Puffin Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
15646|Puffin Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Ashmore Platform / Vulcan Sub-basin.||||||07-FEB-11
15646|Puffin Formation|60378|5|Briefly described|p95, fig 2, p96, 98, 106|Late Cretaceous|Late Cretaceous|Includes interpreted deep marine fan sediments considered to be a reservoir facies.|||||Includes sandstone.|
15646|Puffin Formation|60634|6|Mentioned|p1167 Fig.2,  p1168 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson and Fenelon Formations. Is overlain by Johnson Formation.||
15646|Puffin Formation|61550|6|Mentioned|p495 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||
15646|Puffin Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Age: ~80-65Ma. Geological Province: Arafura and Money Shoals Basin.||||||01-MAR-10
15646|Puffin Formation|63358|5|Briefly described|p4 Fig. 1.3|Masstrichtian|Campanian|See also p133 Fig. 3.71.||||||01-MAR-10
15646|Puffin Formation|64697|5|Briefly described|p84 Fig.2, p88 |Late Cretaceous|Late Cretaceous|||||||
15646|Puffin Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Maastrichtian|Maastrichtian|Bathurst Island Group. Underlies the Johnson Formation, overlies the Fenelon Formation. Mount Ashmore Dome. Interbedded deep-water marine sandstone and claystone.||||||
15646|Puffin Formation|69297|6|Mentioned|p305|Maastrichtian|Campanian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.||Bathurst Island Group||Overlies the Fenelon Formation. Overlain by the Bassett Formation.||
15646|Puffin Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p6, p12|Maastrichtian|Campanian|See also Vulcan: Fig.2, p2. Productive petroleum reservoir. Regionally-developed sandstones form high-quality reservoirs; commonly sealed by Johnson Formation carbonates. Potential gas reservoir in Vulcan Sub-basin.||Bathurst Island Group.||Overlies Wangarlu Formation. Is overlain by Johnson Formation. Correlates with Turnstone Formation.|Lowstand fan sandstones.|12-JUL-16
15646|Puffin Formation|70064|5|Briefly described|Regional Fig. 6; p6. Central: Fig.2; p2|Maastrichtian|Campanian|See also Northern: Fig.2: p1, p3. Yampi: Fig.2. Browse Basin. Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoirs in horsts and tilted fault-blocks in submarine fan sandstones. Potential intraformational seals.||Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||12-JUL-16
15666|Punkerri Sandstone|22922|6|Mentioned|33 fig 2|||||||||
15666|Punkerri Sandstone|23282|1|Redefined|p67||Neoproterozoic|Equivalent to Pound Subgroup in the Adelaide Fold Belt. Original Punkerri Sandstone by Thomson (1969), then redefined as Punkerri Beds by Major (1974), now redefined as Punkerri Sandstone. Of Ungoolya Group, Officer Basin. Age: Neoprot - latest Marinoan.||||||30-SEP-08
15666|Punkerri Sandstone|23818|6|Mentioned|p78|||Contains Ediacara sea pen fossil types.||||||
15666|Punkerri Sandstone|24067|5|Briefly described|p249 Fig.2|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
15666|Punkerri Sandstone|24112|5|Briefly described|p254 Fig.2|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
15666|Punkerri Sandstone|30218|6|Mentioned|p404|||||||||
15666|Punkerri Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
15666|Punkerri Sandstone|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15666|Punkerri Sandstone|31965|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15666|Punkerri Sandstone|31969|6|Mentioned|p9|||||||||
15666|Punkerri Sandstone|31971|6|Mentioned|p6|||See also P8||||||
15666|Punkerri Sandstone|31973|6|Mentioned|p5|||Now Punkerri Beds. Top & bottom not exposed.||||||
15666|Punkerri Sandstone|33655|5|Briefly described|p100|||||||||
15666|Punkerri Sandstone|34535|6|Mentioned|p78|||||||||
15666|Punkerri Sandstone|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
15666|Punkerri Sandstone|42661|6|Mentioned|p130|||||||||
15666|Punkerri Sandstone|43743|6|Mentioned|Fig.2,p33||Neoproterozoic|||||||
15666|Punkerri Sandstone|44133|5|Briefly described|p39|Neoproterozoic|Neoproterozoic|Unconformably underlies Wirrildar beds, Kulyong Volcanics.||||||
15666|Punkerri Sandstone|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Shallow marine sandstone and siltstone.||||||27-APR-05
15666|Punkerri Sandstone|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Shallow marine sandstone and siltstone.||||||06-JUN-05
15666|Punkerri Sandstone|61732|4|Described|p58 Fig. 22, p67|Ediacaran|Ediacaran|Of Ungoolya Group. Previously known as "Punkerri beds" or "Punkerri Fm". Redefined by Morton (1997). Max. thickness: >1200m. In type section. Geol.Prov: Officer Basin. See also p145 Fig. 51.G106.||||||07-FEB-11
15666|Punkerri Sandstone|62453|4|Described|p14, 50|Ediacaran|Ediacaran|Quartzite, sandstone, siltstone, minor conglomerate and carbonate. Overlies disconformably: Wright Hill Formation. Underlies; Wirrildar beds.||||||
15666|Punkerri Sandstone|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate.||||||09-DEC-08
15666|Punkerri Sandstone|65416|6|Mentioned|p144.|Late Proterozoic|Late Proterozoic|||||Is overlain by Wirrildar beds.||
15666|Punkerri Sandstone|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
15666|Punkerri Sandstone|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Ungoolya Group (Rodda beds), Karlaya Limestone, Wright Hill beds. Group description: Marine sandstone, grey indurated mudstone and limestone.||||Said to be equivalent to Wilpena Group||
15666|Punkerri Sandstone|69153|6|Mentioned|500k_geologyp08_lut.csv||Neoproterozoic||||||Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate|
15666|Punkerri Sandstone|70634|4|Described|500k_geolgyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Quartz sandstone, feldspathic sandstone, and siltstone; minor conglomerate.|
15666|Punkerri Sandstone|70790|6|Mentioned|p271|||||||Equivalent to Bonney Sandstone.||
15666|Punkerri Sandstone|70793|4|Described|500k_interpgeop14_lut.csv|Ediacaran|Ediacaran|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-541 Ma (biostrat; inferred)||||Sandstone, reddish brown, flaggy, micaceous to feldspathic, and lesser siltstone|
15666|Punkerri Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
15666|Punkerri Sandstone|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Ungoolya Group.|||Lower purple, red-brown flaggy sandstone; upper red, white feldspathic and quartzose sandstone, interbedded siltstone|
15666|Punkerri Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Officer Basin (Phase 1).|||||Sandstone, reddish brown, flaggy, micaceous to feldspathic, and lesser siltstone.|
15666|Punkerri Sandstone|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 570 Ma-545 Ma|Ungoolya Group||Unconformably overlies Munyarai Formation. Unconformably overlain by the Relief Sandstone.||24-MAR-21
15666|Punkerri Sandstone|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15666|Punkerri Sandstone|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15666|Punkerri Sandstone|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
15671|Puntapunta Formation|23414|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Of Lamil Group, Yeneena Basin.||||||09-DEC-08
15671|Puntapunta Formation|23900|4|Described|p1537 Fig.2|Proterozoic|Proterozoic|Of the Lamil Group. Overlies the Telfer Formation. Overlain by the Wilki Quartzite. Geological Province: Paterson orogen.||||||
15671|Puntapunta Formation|24194|5|Briefly described|p900 Fig.3|Neoproterozoic|Neoproterozoic|Dolomite, limestone. Parent: Lamil Group. Geological Province: Paterson Orogeny.||||||09-DEC-08
15671|Puntapunta Formation|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Variation of Punta Punta?||||||
15671|Puntapunta Formation|37212|6|Mentioned|Table 1|||||||||
15671|Puntapunta Formation|43278|4|Described|p346,Fig.2.|Neoproterozoic|Neoproterozoic|Of Yeneena Group.||||||09-DEC-08
15671|Puntapunta Formation|43867|5|Briefly described|p199,201|||||||||
15671|Puntapunta Formation|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic|Chin et al. (1982). 2000 m. Dolomite, limestone, calcarenite; minor sandstone, siltstone, shale. Northeastern zone of Yeneena Basin, conformably overlies Telfer Formation, conformably overlain by Wilki Quartzite.|| ||||06-MAR-18
15671|Puntapunta Formation|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
15671|Puntapunta Formation|60470|5|Briefly described|p4, Fig. 2, p9, 10-11|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Lamil Group. Conformably overlies Malu Formation. Ferruginized, laminated to thinly bedded sequence of dark grey dolomitic sandstone, grey dolomitic siltstone, and rare limestone, very fine grained pale brown dolomitic sandstone, chert, and shale.||||||
15671|Puntapunta Formation|62453|3|Fully described|p5 Fig. 3, 69|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Lamil Group. Conformably overlies Malu Formation. Conformably overlain by Wilki Formation. Thickness 1.5km. Sandstone, siltstone, chert, limestone, shale.||||||
15671|Puntapunta Formation|64580|4|Described|map legend||Neoproterozoic|Of Lamil Group. Dolarenite interbedded with dolomite, siltstone, and shale; thinly bedded, fine to medium grained.||||||09-DEC-08
15671|Puntapunta Formation|64777|5|Briefly described|p3 Fig.4, |Neoproterozoic|Neoproterozoic|||Of the Lamil Group|||Shale, carbonate rocks, and turbidite units.|
15671|Puntapunta Formation|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin. Age: c. 845 Ma, maximum depositional age, SHRIMP U-Pb detrital zircon; and, 835+/-4 Ma, minimum age for sedimentation, monazite at Duke Cu-Pb-Zn prospect, SHRIMP U-Pb zircon.|see comments|Lamil Group||Overlies Malu Formation. Is overlain by Wilki Formation.||
15671|Puntapunta Formation|65454|4|Described|p7-9, p11, p13, p19, p23, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of Lamil Group. Dominantly clastic carbonate rocks interbedded with siltstone and shale; minor chert; commonly dolomitic and arenaceous. Max depositional age of ~850 Ma based on detrital zircons.||||||
15671|Puntapunta Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Lamil Group. Overlies Malu Formation. Overlain by Wilki Formation. Dominantly dolarenite interbedded with dolomite, siltstone and shale. Thinly bedded and fine- to medium-grained. Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
15671|Puntapunta Formation|65826|4|Described|p1, p13, p17.|Neoproterozoic|Neoproterozoic|About 1.5 km thick in the northwest part of PATERSON map area. Hosts the North Magnetic gold prospect in thin auriferous stockworks of quartz-pyrite-carbonate veins.||Unit in Lamil Group.||Overlies Malu Formation. Is overlain conformably by the Wilki Formation.|A laminated to thinly bedded sequence of dolarenite interbedded with dolomite, siltstone and shale. South of Mount Crofton Granite it is hornfelsed, yellow, pink and brown, thinly bedded, fine- to medium-grained dolomite interbedded with siltstone.|
15671|Puntapunta Formation|67202|4|Described|p7, p43, p59, p117, p157, p175, p177|Neoproterozoic|Neoproterozoic|See also p183, p190-191, p196, p198-199, p203, p208, p280. Yeneena Basin. An aquifer supplying water to the Telfer mining community. Up to 1.5km thick. Deposition on a carbonate-dominated shelf. Conductance image. Hosts the Dromedary (also known as Duke) Zn deposit. Associated with the O'Callaghans W(-Zn-Pb-Cu) deposit. Appears as Punta Punta Formation on p190.||Lamil Group.||Conformably overlies Malu Formation. Is intruded by O'Callaghans Granite. Is interpreted to be conformably overlain by Wilki Formation.|Dolomitic siltstone, rare limestone, dolomitic sandstone, chert and shale.|
15671|Puntapunta Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Yeneena Basin.||Lamil Group.||||
15671|Puntapunta Formation|69590|4|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.csv.|1000-541 Ma (inferred)|Unit of Lamil Group.|||Dolarenite interbedded with dolomite, siltstone, and shale; thinly bedded, fine to medium grained|
15671|Puntapunta Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite, sandstone, shale, dolarenite|
15671|Puntapunta Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Neoproterozoic|Yeneena Basin.||Lamil Group.|||Dolarenite interbedded with dolomite, siltstone, and shale; thinly bedded, fine to medium grained.|
15671|Puntapunta Formation|73345|6|Mentioned|p228|||Yeneena Basin[?].||||||
15689|Pussy Cat Group|30385|6|Mentioned|p8|||||||||
15689|Pussy Cat Group|30388|4|Described|Table 1|||Middle Proterozoic age. Equivalent? to Tollu Group.||||||09-DEC-08
15689|Pussy Cat Group|30390|4|Described|p49|||See also P50||||||
15689|Pussy Cat Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
15689|Pussy Cat Group|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup||||||
15689|Pussy Cat Group|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|36551|6|Mentioned|Table 31|||||||||
15689|Pussy Cat Group|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15689|Pussy Cat Group|36886|4|Described|p196|||||||||
15689|Pussy Cat Group|37707|6|Mentioned|p24|||||||||
15689|Pussy Cat Group|44139|5|Briefly described|p284, Table 3-16|||Of Bentley Supergroup. ~300m. Basalt, minor rhyolite. May be equivalent to Tollu Group.|| ||||10-SEP-12
15689|Pussy Cat Group|45149|5|Briefly described|p19|||||||||
15689|Pussy Cat Group|50607|6|Mentioned|p3.2|||Geological Province: Musgrave Block.||||||
15689|Pussy Cat Group|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Volcanics. Geological Province: Musgrave Province.||||||
15689|Pussy Cat Group|61864|6|Mentioned|p18 fig 4|||Volcanics.||||||
15689|Pussy Cat Group|62453|6|Mentioned|p15|||Of the Bentley Supergroup.||||||
15689|Pussy Cat Group|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
15689|Pussy Cat Group|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup. Rhyolite, dacite, ignimbrite, basalt, volcaniclastic sedimentary rock, sandstone, and conglomerate.||||||09-DEC-08
15689|Pussy Cat Group|65256|6|Mentioned|p14, p30|||Lateral equivalent of the Tollu Group; may be equivalent to Tjuninanta Formation (Tjauwata Group). Includes Glyde Formation.||||||
15689|Pussy Cat Group|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.|||Includes Glyde Formation.|||11-APR-12
15689|Pussy Cat Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes Glyde Formation.|||
15689|Pussy Cat Group|67375|4|Described|p7, pp8-9 Fig.5, p38 Table 1, pp46-47.|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, Musgrave Region. May be laterally equivalent to Tollu Group.|1071-1065 Ma.|Unit in Bentley Supergroup.|Includes Kathleen Ignimbrite and Glyde Formation.|Overlies Scamp rhyolite (informal name). Is overlain by Cassidy Group.|Metabasalts and intercalated metasedimentary rocks.|
15689|Pussy Cat Group|67553|5|Briefly described|p8,11,17,40-42,48-50,59,94,97-98|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Blackstone Sub-basin, Bentley Sub-basin. [Also misspelt as Pussycat Group on p98]. Affected by an episode of syn- to post-depositional folding. Outcropping portions up to 3000m thick, however full thickness is uncertain.|1071-1065 Ma|Unit of Bentley Supergroup.|Includes Glyde Formation and Kathleen Ignimbrite.|Conformably overlain by Cassidy Group/Wururu Rhyolite.||06-AUG-19
15689|Pussy Cat Group|68995|4|Described|p3-4, p7-9, p15, p24, p27 Tb.2, p45-46|Stenian|Stenian|Talbot Sub-basin. Age based on the Giles Event which occurred as this unit was deposited. At least 3500m thick based on outcrop; 2100m of this is basaltic lava flows.|c. 1085-1040 Ma|Bentley Supergroup|Glyde Formation, Kathleen Ignimbrite|Overlies the Mount Waugh rhyolite (apparently conformably) and the Kaarnka Group. (Maybe unconformably) overlain by the Cassidy Group.|Bimodal volcanic rocks with less common sedimentary rocks that shallowly dip.|
15689|Pussy Cat Group|68996|5|Briefly described|p5, 7, p32-39, p47, 50, 65|Mesoproterozoic|Mesoproterozoic||1071 +/- 5 Ma (SHRIMP)|Bentley Supergroup|Includes Kathleen Ignimbrite, Glyde Formation|||
15689|Pussy Cat Group|69003|5|Briefly described|p37, p51-52|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province.|1071 +/- 5 Ma - 1065 +/- 5 Ma.|Bentley Supergroup.|Glyde Formation, Kathleen Ignimbrite.|Is overlain (probably unconformably) by Cassidy Group.||
15689|Pussy Cat Group|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1071-1047 Ma|Of the Bentley Supergroup.|Includes Kathleen Ignimbrite.||Comprises quartz-feldspar-porphyritic rhyolite; volcaniclasitc rhyolite; diamictite; sandstone and siltstone to mudstone; rhyolite.|
15689|Pussy Cat Group|69091|4|Described|p30 Fig.3.5, p41 Fig.3.8, see comments|||Talbot Sub-basin, Musgrave Province. Bimodal volcanic rocks and less common sedimentary units dip shallowly (less than 30 degrees) to south and southwest, and form continuous packages that can be traced for over 100 km. See also p52 Fig.4.1, p54 Fig.4.2, p59 Fig.4.6, p71 Fig.4.14, p75, p81 Fig.4.17, p106 Fig.5.7a, p107 Fig.5.8a, p108 Fig.5.9, p109 Fig.5.10, p115 Fig.5.14, p117 Fig.5.15, p119 Fig.5.16, p131 Fig.6.1, p133, p144, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||Bentley Supergroup|Kathleen Ignimbrite, Glyde Formation|Overlies Mount Palgrave and Kaarnka Groups; is overlain by Cassidy Group.|Continuous packages of bimodal volcanic rocks and less common sedimentary units.|
15689|Pussy Cat Group|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Bentley Supergroup|Glyde Formation, Kathleen Ignimbrite||Sedimentary siliciclastic (sandstone, siltstone, mudstone; rare conglomerate of basalt, rhyolite and granite cobbles), evaporites, diamictite; interbedded basalt, basaltic andesite; porphyritic quartz-feldspar rhyolite; subvolcanic intrusion - mafic|
15689|Pussy Cat Group|69655|5|Briefly described|p3, p6|Stenian|Stenian|Musgrave Region.|c. 1090-1040 Ma|Bentley Supergroup||||
15689|Pussy Cat Group|69729|5|Briefly described|p66 Fig.1, p68, p70, p80, p82|||Talbot Sub-basin, Musgrave Province.||Bentley Supergroup.|Glyde Formation, Kathleen Ignimbrite.|Overlies the Mount Palgrave Group. Is overlain by the Cassidy Group.||
15689|Pussy Cat Group|70095|5|Briefly described|p16-19|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. [Name is hyphenated on p16]. Thickness of rhyolitic package: 0.9km; thickness of basaltic package: 2.1km. Strike length: over 200km, over multiple eruptive events. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||Unit of Bentley Supergroup.|Includes Kathleen Ignimbrite and Kaarnka Group.|Overlain by Cassidy Group/Wururu Rhyolite. Underlain by Mount Palgrave Group/Mount Waugh rhyolite.||
15689|Pussy Cat Group|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|1071-1047 Ma.|Bentley Supergroup.|Glyde Formation.|Overlies Mount Palgrave Group. Is overlain by Cassidy Group.||
15689|Pussy Cat Group|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup.|Glyde Formation.||Rhyolite, vesicular and amygdaloidal basalt, basaltic andesite, andesite, medium- to fine-grained siliciclastic rocks, rare calc-silicate rocks, evaporite horizons and microbialites.|
15689|Pussy Cat Group|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1049 Ma - 1077 Ma (Inferred)|Bentley Supergroup|Includes Kathleen Ignimbrite||Vesicular and amygdaloidal basalt and minor basaltic andesite with minor siliciclastic interbeds. Porphyritic quartz-feldspar rhyolite with rounded quartz and alkali feldspar phenocrysts; fine grained micrographic to felsitic groundmass.|
15689|Pussy Cat 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 Glyde Formation and Kathleen Ignimbrite.||Vesicular and amygdaloidal basalt, and minor basaltic andesite; locally plagioclase porphyritic; quartz-feldpsar-porphyritic rhyolite, interbedded sandstone and medium- to fine-grained siliciclastic rocks.|
15689|Pussy Cat Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Shown as Pussycat Group p10.||Bentley Supergroup||||20-APR-20
15689|Pussy Cat Group|70831|5|Briefly described|p3, p5|||Musgrave Province.||Bentley Supergroup||||
15689|Pussy Cat Group|71170|5|Briefly described|p5-p6|||Talbot Sub-basin. Emplaced during the Giles Event.||Bentley Supergroup||||
15689|Pussy Cat Group|71210|6|Mentioned|p5|||Talbot Sub-basin.||||||
15689|Pussy Cat Group|71211|4|Described|i-iii, vii, ix-xi, xiii, p1|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin. Magmas of this group were evolved, anhydrous, metaluminous A-types that were enriched in REE. On the basis of geochemistry this Group is interpreted to have been formed primarily by mantle derived magmas. See also p6 fig 1.3, p7 fig 1.4, p11, p13  p24 fig 2.1, p25, p26, p63, p81-p84, p86, p88-p89 fig 3.3, p94, p96, p99 fig 3.7, p102-p108, p110, p112, p113, p115-p117, p119-p120, p135, p136 fig 4.1, p208-p210, p212, p215-p216, p234, p265-p266.|1085-1040 Ma|Bentley Supergroup|Includes the Rowland Suite, Kathleen Ignimbrite, Glyde Formation and (the Cleghorne Formation).|Conformably overlies the Mount Palgrave and Kaarnka Groups. Overlain by the Cassidy and Mission Groups.|Rhyolitic magmas.|01-SEP-17
15689|Pussy Cat 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). 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.||Unit of Bentley Supergroup.|Includes Glyde Formation, Kathleen Ignimbrite.||Vesicular and amygdaloidal basalt, and minor basaltic andesite; locally plagioclase porphyritic; epidotized; quartz-feldspar-porphyritic rhyolite; diamictite, conglomerate, interbedded sandstone, siltstone and mudstone.|
15689|Pussy Cat Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Four informal sub-units specified [Unclear how these might relate to the 4 named units that form the Pussy Cat Group].|||Includes Glyde Formation, Kathleen Ignimbrite.||Porphyritic rhyolite; subvolcanic. Matrix- to clast-supported conglom.; mainly basalt cobbles; interbedded w med. to fine siliciclastics. Diamictite; subrounded/angular mafic/felsic volc. clasts. Med. to fine siliciclastics, interbedded w basalt.|
15689|Pussy Cat Group|72094|4|Described|p3 Fig 2, p4, 7, 13|Stenian|Stenian|Talbot Sub-basin, Bentley Basin. Intruded by Warakurna Supersuite intrusions with U-Pb 1071+\-5, 1063+\-8 and 1049+\-8 Ma zircon ages (Smithies et al., 2013b).||Unit of Bentley Supergroup.||Underlain, and intruded by fine- to medium-grained intrusions of the Warakurna Supersuite.|Vesicular and amygdaloidal basalt, locally with voluminous volcaniclastic rhyolite and intercalated fine- to coarse-grained volcaniclastic and siliciclastic rocks.|
15689|Pussy Cat Group|72443|5|Briefly described|p737-740, p742, p753|||Talbot Sub-basin.|1081 +/- 9 to 1070 +/- 11 Ma (SHRIMP U-Pb)|Bentley Supergroup|Includes the Glyde Formation and the Kathleen Ignimbrite.|Overlies the Mount Palgrave Group. Overlain by the Cassidy Group.|Dominantly ignimbrite and overlying amygdaloidal basaltic lavas and interlayered volcaniclastic sedimentary rocks.|
15689|Pussy Cat Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Talbot Sub-basin.||Bentley Supergroup||||
15703|Pyradie Formation|23045|6|Mentioned|291 fig 8|||Of the Fortescue Group.||||||16-JAN-07
15703|Pyradie Formation|23570|4|Described|p93|Archean|Archean|See also  p238 App. 1.  Formerly the Pyradie Pyroclastic Member of de la Hunty (1965).  Correlated as lateral equivalent of the Tumbiana Formation.  Overlain by  Bunjinah Formation; underlain by Boongal Formation.   Geological Province: Pilbara Craton||||||22-APR-09
15703|Pyradie Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlain by Boongal Formation. Geological Province Hamersley Basin.||||||07-NOV-08
15703|Pyradie Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Boongal Formation. Overlain by Bunjinah Formation. Age: c. 2715 Ma. Tuff and volcanic breccia. Geological Province: Hamersley Basin.||||||07-NOV-08
15703|Pyradie Formation|42471|5|Briefly described|p6, p4|||Equivalent to Pyradie Pyroclastic Member of Mount Jope Volcanics (1965, 1968).||||||
15703|Pyradie Formation|42472|5|Briefly described|Map legend|Archean||||||||07-NOV-08
15703|Pyradie Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
15703|Pyradie Formation|42744|4|Described|p4|||||||||
15703|Pyradie Formation|43119|4|Described|p7|||Of the Fortescue Group.||||||16-JAN-07
15703|Pyradie Formation|43262|5|Briefly described|Map Legend||Archean|Of Fortescue Group.||||||08-APR-09
15703|Pyradie Formation|43290|4|Described|p5||Archean|Of the Fortescue Group.||||||07-NOV-08
15703|Pyradie Formation|60706|5|Briefly described|p625 Fig.3|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
15703|Pyradie Formation|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
15703|Pyradie Formation|62129|3|Fully described|p6, p7, p21, p24|Archaean|Archaean|Of Fortescue Group. Conformably underlain by Boongal Formation, conformably overlain by Bunjinah Formation. Thickness: 1000m. Geological Province: Hamersley Basin. See p7 for lithological information.||||||17-DEC-12
15703|Pyradie Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Metamorphosed pyroxene spinifex-textured basaltic flows and pillow lava; metamorphosed volcanic sandstone and minor chert.||||||01-JUL-14
15703|Pyradie Formation|63367|6|Mentioned|p230, p232 Fig.2.|||||Unit in Fortescue Group.||Lateral facies equivalent to Tumbiana Formation (Hamersley Basin).|Subaqueous basaltic lavas; subaerial basalt flows and airfall volcanic tuff; spinifex-textured basalt and komatiite.|
15703|Pyradie Formation|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Geological province: southern Hamersley Basin. Ultramafic and komatiitic.||||||07-FEB-11
15703|Pyradie Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Pyroxene spinifex-textured basaltic flows and pillow lava; mafic volcaniclastic rock; minor chert; local komatiite; metamorphosed.||||||09-DEC-08
15703|Pyradie Formation|64724|5|Briefly described|p42 Fig. 3|Neoarchean|Neoarchean|Hamersley Basin unit.||Of Fortescue Group.||||02-APR-12
15703|Pyradie Formation|66217|5|Briefly described|p45.|||Fortescue Basin.||Unit in Fortescue Group.|||Subaqueous basaltic to komatiitic lavas and volcaniclastic rocks.|
15703|Pyradie Formation|66685|5|Briefly described|p229-230|Archean|Archean|Up to 800m thick. Suggested marine origin. Considered the lateral equivalent of the Tumbiana Formation in the south Pilbara sub-basin. See: Thorne et al. 1991, Thorne and Trendall 2001.||||Lateral equivalent of the Tumbiana Formation.|Consists of pyroxene, spinifex-textured basalt flows and pillow lavas, hyaloclastite, komatiite, sandstone, argillite, and minor chert.|
15703|Pyradie Formation|67025|6|Mentioned|p322 Table 3.|||Hamersley Basin. Mean bulk susceptibility of this and other units is discussed in this article.||||||
15703|Pyradie Formation|67201|5|Briefly described|p28-30|||In northern Pilbara Craton, Fortescue Basin, South Pilbara Sub-basin.||Fortescue Group||Equivalent to Tumbiana Formation.||
15703|Pyradie Formation|67229|5|Briefly described|p2 Fig.1, p4|||South Pilbara Sub-basin, Fortescue Basin.||Fortescue Group.||Equivalent to Tumbiana Formation.|Dominated by komatiite, komatiitic basalt, basalt; minor chert and tuffaceous argillites.|
15703|Pyradie Formation|68035|5|Briefly described|p292|Neoarchean|Neoarchean|A 1 km thick marine unit in the S Pilbara.||||Correlated with Tumbiana Formation.|Komatiite, komatiitic basalt, hyaloclastite, argillite, and chert.|
15703|Pyradie Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Fortescue Group.|||Pyroxene-spinifex basaltic flows and pillow lava with mafic volcaniclastic rock; minor chert and local komatiite; metamorphosed.|06-MAY-14
15703|Pyradie Formation|69080|5|Briefly described|p687, p693|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Overlies Boongal Formation. Is overlain by Bunjinah Formation.||
15703|Pyradie Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Pyroxene spinifex-textured basaltic flows and pillow lava; mafic volcaniclastic rock; minor chert; local komatiite; metamorphosed.|
15703|Pyradie 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. 2719 Ma|Unit of Fortescue Group.|||Pyroxene spinifex-textured basaltic flows and pillow lava; mafic volcaniclastic rock; minor chert; local komatiite; metamorphosed|
15703|Pyradie Formation|69299|5|Briefly described|p16|||South Pilbara sub-basin||||Stratigraphically equivalent to Tumbiana Formation.|Komatiitic volcanic rocks.|
15703|Pyradie Formation|69301|5|Briefly described|p17 Fig.6, p18 Fig.7|||Pilbara Craton. Fortescue Basin. South Pilbara Sub-basin, Sequence 3.||Fortescue Group||||
15703|Pyradie Formation|69411|5|Briefly described|p283|Neoarchean|Neoarchean|Laterally equivalent to Tumbiana Formation. Deeper shelf depositional environment (Thorne and Trendall 2001).|||||Pillow lava, hyaloclastite, komatiite, minor chert and tuffaceous argillite.|
15703|Pyradie Formation|69792|6|Mentioned|p1096 Fig.1|||Appears to be shown as equivalent to Tumbiana Formation.||Unit in Fortescue Group.||||22-JUN-20
15703|Pyradie Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2735-2629 Ma|||||
15703|Pyradie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||ash tuff, chert, komatiite, pyroxene spinifex-textured basalt|
15703|Pyradie Formation|71803|4|Described|p365-p369, p371, p375, p379-p380, p387|Neoarchean|Neoarchean|Pilbara Craton. Geochemistry discussed. An additional age of 2715 +/- 6 Ma is derived from Arndt et al, 1991.|2724+/- 5 Ma (Blake et al, 2004)|||Lateral equivalent to the Tumbiana Formation.|Basalts and rare Al-depleted komatiites.|
15703|Pyradie Formation|71808|6|Mentioned|p8|||Hamersley Province.||||Equivalent to the Tumbiana Formation.||
15703|Pyradie Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|South Pilbara Sub-basin, Fortescue Basin.||Fortescue Group, sequence 4|||Pyroxene spinifex-textured basaltic flows and pillow lava with mafic volcaniclastic rock; minor chert and local komatiite; metamorphosed.|
15703|Pyradie Formation|72712|6|Mentioned|p8, p9 Fig.5, p10 Fig.6.|Neoarchean|Neoarchean|Indicated on p10 Fig.6 as comprising submarine high Mg basalt and komatiite. Approximately 1km thick in the study area.||Fortescue Group||Conformably overlies Boongal Formation and underlies Bunjinah Formation and is equivalent to Tumbiana Formation.|Includes pyroxene spinifex-textured basalt and pillow basalt interbedded with hyaloclastite breccia, volcaniclastic rock, mudstone and chert. Includes a prominent serpentinized komatiite flow in the middle of the formation.|14-JAN-21
15703|Pyradie Formation|73538|6|Mentioned|p2, p4, p6-7|Neoarchean|Neoarchean|Written as Pyradie Formation / Tumbiana Formation. Ages of 2715 +/- 6 Ma and 2724 +/- 5 Ma were reported by Mole et al. (2018) for these units. [Written as Pyradie komatiites on p2, p6-7].|2715 +/- 6 Ma, 2724 +/- 5 Ma|Fortescue Group||Underlain by Kylena Formation / Boongali Formation. Overlain by Maddina Formation / Bunjinah Formation.|Mafic volcanics including komatiites.|
15714|Quail Formation|12471|6|Mentioned|p475 Fig.2, pp482-483.|Early Carboniferous|Early Carboniferous|Two sandstone intervals show reservoir potential.||||Overlies Moogooree Limestone.||
15714|Quail Formation|12729|6|Mentioned|p.15, 27, 28.||Early Carboniferous|Gascoyne Platform. Used in relation to limestone, sandstone, and claystone in Gnaraloo 1 and possibly Warroora 1.||||?Unconformably overlain by Lyons Group.|Braided-fluvial and alluvial-fan sediments (limestone, sandstone, and claystone).|
15714|Quail Formation|12733|6|Mentioned|p554 Fig.2.|Carboniferous|Carboniferous|Visean-Namurian.||||Overlies Yindagindy Formation.||
15714|Quail Formation|13615|3|Fully described|p4, p15-p16, p32, p34|Visean|Visean|Peedamullah Shelf. Up to 100m thick. Intersected in Topaz 2 and Amber 1 drillholes. Type section occurs in Quail 1: 2100-2452m. Sparse fauna and flora.Deposited in a marine shelf environment. See also p41-p42, p46, p53, p55, p75, p79-80, p83-p85, p87, p103 App.3.|c. 330 Ma|||Overlies the Moogooree Limestone. Unconformably overlain by the Lyons Group.|Sandstone, lithic to quartz wacke, grey siltstone, variably calcareous and minor thin limestone interbeds.|09-FEB-19
15714|Quail Formation|14228|5|Briefly described|p5 Fig.2, p6 fig3, p7, p18|Visean|Tournaisian|Merlinleigh Sub-basin. Possible seal for Munabia Formation.||||Overlies Moogooree Limestone. Equivalent to Williambury and Yindagindy Formations.|Siltstone and sandstone.|
15714|Quail Formation|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
15714|Quail Formation|23726|5|Briefly described|p13|Early Carboniferous|Early Carboniferous|See also p7 Fig 2b. Geological Province: Carnarvon Basin.||||||
15714|Quail Formation|24390|5|Briefly described|p19 Fig. 10||Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
15714|Quail Formation|35282|6|Mentioned|Fig.2|||||||||
15714|Quail Formation|40617|2|Defined|p4|Early Carboniferous|Early Carboniferous|||||||
15714|Quail Formation|41271|3|Fully described|p62|||||||||
15714|Quail Formation|41438|6|Mentioned|p103|||||||||
15714|Quail Formation|41441|5|Briefly described|p151|||||||||
15714|Quail Formation|41443|4|Described|p163|||||||||
15714|Quail Formation|42116|5|Briefly described|Fig.1 P5|||||||||
15714|Quail Formation|43566|6|Mentioned|p413|||||||||
15714|Quail Formation|49942|5|Briefly described|p4 Fig.3|Carboniferous|Carboniferous|Geological Province: Merlinleigh Sub-basin.||||||
15714|Quail Formation|50085|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
15714|Quail Formation|60384|5|Briefly described|p244, p243 Fig 2a, p260 table 2||Early Carboniferous|Merlinleigh Sub-Basin, Southern Carnarvon Basin.  Marine siliciclastics. Gas show at top in Gnaraloo-1 well (1967).||||||15-NOV-12
15714|Quail Formation|60725|5|Briefly described|p29 Fig.2; p33 Fig.4; p35-36 Figs.5,6.|Carboniferous|Carboniferous|||||||
15714|Quail Formation|61023|5|Briefly described|p34 Fig. 14|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
15714|Quail Formation|64972|6|Mentioned|p617 Fig. 5|Carboniferous|Carboniferous|||||||
15714|Quail Formation|65382|6|Mentioned|p717 App. 2|Visean|Visean|Carnarvon Basin. 327 Ma||||||
15714|Quail Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes reddish brown medium-grained sandstone.|
15714|Quail Formation|67200|5|Briefly described|p7 fig 5,p18 table 1, p48, p55, app 2 p7|Carboniferous|Carboniferous|Thermal conductivity of 3.28 W/mK||||Overlies Moogooree Limestone|Parallel bedded silstone and medium grained sandstone.|
15714|Quail Formation|69029|6|Mentioned|p326|Namurian|Visean|Of onshore Carnarvon Basin.||||Overlain by Lyons Group. Underlain by Yindagindy Formation.||
15714|Quail Formation|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Middle Carboniferous|Early Carboniferous|Carnarvon Basin. Deposited as a shore-face or marine-shelf deposit. See also Ch3 p23-p25, Ch3 p35, Ch3 p67-p68, Ch3 p73.||||Overlies the Yindagindy Formation.|Siltstone and sandstone.|
15714|Quail Formation|71146|5|Briefly described|p6, p34|Visean|Visean|Southern Carnarvon Basin.||||Unconformably overlies the Yindagindy Formation.|Sandstone.|
15714|Quail Formation|73117|6|Mentioned|p15, p35|Serpukhovian|Visean|Southern Carnarvon Basin. G. maculosa Zone [palynology] is present||||||
15715|Quailing Laterite|42280|6|Mentioned|p45|||||||||
15767|Quinnanie Shale|12733|6|Mentioned|p565.|Early Permian|Early Permian|Contains significant hydrocarbon source rocks.||Unit in Byro Group.||||
15767|Quinnanie Shale|14228|5|Briefly described|p8, p18|Permian|Permian|Forams indicate hyposaline high-latitude interior sea.||Byro Group||||06-OCT-16
15767|Quinnanie Shale|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
15767|Quinnanie Shale|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
15767|Quinnanie Shale|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
15767|Quinnanie Shale|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
15767|Quinnanie Shale|23726|5|Briefly described|p60|Early Permian|Early Permian|Of Byro Group. Overlying unit Wandagee Formation. Underlying unit Cundlego Formation. Geological Province: Carnarvon Basin.||||||
15767|Quinnanie Shale|23815|4|Described|p286|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Minilya Subgroup. Overlying unit: Wandagee Formation (conformable). Underlying unit: Cundlego Formation (conformable). Max. thickness: 119 m.||||||27-APR-05
15767|Quinnanie Shale|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
15767|Quinnanie Shale|31251|6|Mentioned|p68|||Refers Thomas (1958), WcWhae et al. (1958)||||||
15767|Quinnanie Shale|32648|6|Mentioned|p32|||in Byro Gp.||||||
15767|Quinnanie Shale|33710|6|Mentioned|Fig.1|||||||||
15767|Quinnanie Shale|34277|6|Mentioned|Table 1|||Permian||||||
15767|Quinnanie Shale|34532|6|Mentioned|p225|||Byro Gp.||||||
15767|Quinnanie Shale|35282|6|Mentioned|Fig.30|||||||||
15767|Quinnanie Shale|36257|6|Mentioned|Table 2.1|||||||||
15767|Quinnanie Shale|36890|3|Fully described|p286|||||||||
15767|Quinnanie Shale|37294|6|Mentioned|p100|||||||||
15767|Quinnanie Shale|37304|6|Mentioned|p55|||||||||
15767|Quinnanie Shale|37549|6|Mentioned|Fig.9|||||||||
15767|Quinnanie Shale|39316|6|Mentioned|Fig.2|||||||||
15767|Quinnanie Shale|39974|6|Mentioned|p113|||||||||
15767|Quinnanie Shale|40617|6|Mentioned|Fig.1|||||||||
15767|Quinnanie Shale|41049|6|Mentioned|p37|||||||||
15767|Quinnanie Shale|41271|3|Fully described|p97|||||||||
15767|Quinnanie Shale|41438|6|Mentioned|Fig.11|||||||||
15767|Quinnanie Shale|42116|5|Briefly described|p43|||See also Fig.17||||||
15767|Quinnanie Shale|42392|6|Mentioned|p119|||Byro Group||||||
15767|Quinnanie Shale|42473|6|Mentioned|p65|||||||||
15767|Quinnanie Shale|42540|6|Mentioned|Table 2 P314|||||||||
15767|Quinnanie Shale|42654|6|Mentioned|p25|||||||||
15767|Quinnanie Shale|42994|6|Mentioned|p78|||||||||
15767|Quinnanie Shale|43015|5|Briefly described|Table 1,p319|||||||||
15767|Quinnanie Shale|44344|14|Not recorded|p.13-14,opp.4, map||Artinskian|Artinskian; fm. of Minilya Subgroup (Byro Group). Grades laterally into Cundlego Formation. (G50-1).||||||
15767|Quinnanie Shale|44345|14|Not recorded|map legend||Artinskian|Artinskian.||||||
15767|Quinnanie Shale|44532|14|Not recorded|p.8|||Equiv. to upper part of Cundlego Formation.||||||
15767|Quinnanie Shale|44537|14|Not recorded|map legend||Artinskian|||||||
15767|Quinnanie Shale|44657|14|Not recorded|p.5,6,9,16|||||||||
15767|Quinnanie Shale|44994|6|Mentioned|Fig.7|||Perm. Byro Gp.||||||
15767|Quinnanie Shale|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||01-JUN-06
15767|Quinnanie Shale|45016|2|Defined|p159-162||Artinskian|Tb, p.124,125,138,155,157,164,165,167,171,181.||||||
15767|Quinnanie Shale|48610|14|Not recorded|Pl.1|||||||||
15767|Quinnanie Shale|48831|14|Not recorded|p.9,23,24,35,41|||||||||
15767|Quinnanie Shale|48848|14|Not recorded|p.33,37,38,42,46|||||||||
15767|Quinnanie Shale|48858|14|Not recorded|p.5-16|||Intermittent turbulence during deposition, i.e. deltaic. (G50-1/Norton). Pl.1,2.||||||
15767|Quinnanie Shale|49644|5|Briefly described|Table|||||||||
15767|Quinnanie Shale|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of Byro Group. Overlies Cundlego Formation. Overlain by Wandagee Formation. Geological Province: Southern Carnarvon Basin.||||||
15767|Quinnanie Shale|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||
15767|Quinnanie Shale|64580|5|Briefly described|map legend|||Of Middle Byro Group. Interbedded black mudstone, siltstone, and fine-grained sandstone.||||||15-DEC-08
15767|Quinnanie Shale|64974|5|Briefly described|p147 Fig. 5|Kungurian|Kungurian|Of Cundlego Formation. Geological Province: Carnarvon Basin.||||||24-JUN-09
15767|Quinnanie Shale|67200|5|Briefly described|p7 fig 5, |Kungurian|Artinskian|||||Overlies Cundlego Formation, overlain by Wandagee Formation|Shale/siltstone.|
15767|Quinnanie Shale|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.||Grades laterally into upper Cundlego Formation.|Comprises black shale, coarsening upward to grey siltstone.|27-AUG-15
15767|Quinnanie Shale|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Cundlego Formation, Bulgadoo Shale and Wandagee Formation as a single unit.||Of the Byro Group.|||Interbedded black mudstone, siltstone and fine-grained sandstone.|06-MAY-14
15767|Quinnanie Shale|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
15767|Quinnanie Shale|70795|5|Briefly described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group||Grades into upper Cundlego Formation|Black shale, coarsening upward to grey siltstone.|
15767|Quinnanie Shale|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, greywacke, shale|
15767|Quinnanie Shale|72910|4|Described|p10-11, p23, p30, p38, p41.|Kungurian|Kungurian|Thickness 15-135m. Type section: Minilya River, north of Wandagee Hill, 23d44m10sS, 114d25m20sE. Misspelt as Quininie Shale p18. Said to be Artinskian age p38.||Byro Group||Conformably overlies and laterally gradational into Cundlego Formation. Underlies Wandagee Formation (conformably), Nalbia Sandstone.|Black shale, with grey siltstone in upper part.|
15802|Raggedy Member|30562|4|Described|Appendix p38|||See also P9. Archaean age. Of Naganyer Formation.||||||27-NOV-09
15802|Raggedy Member|43162|6|Mentioned|6|||||||||
15830|Ranford Formation|22496|3|Fully described|p11||Neoproterozoic|Of the Duerdin Group. Conformably overlies the Moonlight Valley Tillite.  Inferred to be conformable on the Redbank Yard Formation to the south.  Geological Province:  Wolfe Basin.||||||16-AUG-04
15830|Ranford Formation|22537|5|Briefly described|37|Proterozoic|Proterozoic|||||||
15830|Ranford Formation|22547|4|Described|p28||Neoproterozoic III|Of the Duerdin Group. Geological province:  Wolfe Creek Basin. Thickness: 600 m. Overlies Moonlight Valley Tillite.||||||14-NOV-06
15830|Ranford Formation|22649|6|Mentioned|p 143|||Rb-Sr age: 672+/-70 Ma,   p143.||||||27-NOV-06
15830|Ranford Formation|22777|5|Briefly described|Map|||Of the Duerdin Group.  In the Wolfe Basin.||||||27-NOV-06
15830|Ranford Formation|23621|4|Described|p33|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Duerdin Group. Geological Province: Wolfe Basin.  Max. thickness: 500 m.||||||
15830|Ranford Formation|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
15830|Ranford Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
15830|Ranford Formation|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Duerdin Group. Conformably overlain by Mount Forster Sandstone; conformably overlies Moonlight Valley Tillite; overlies the Illjara Sandstone disconformably. Geological Province: Wolfe Basin. Max Thickness: 500m.||||||09-MAR-05
15830|Ranford Formation|28255|3|Fully described|p76, Tb. 11 (opp. p8), p110|Adelaidean|Adelaidean|Of Duerdin Gp. Includes Jarrad Sst and Johnny Cake Sst Mbrs. Subdivided by Pontifex et al (1968): Bucket Spring, Beasly Knob and Ernie Lagoon Members. Ferruginous and laminated siltstones/sandstones sequence; claystone, "zebra-stone". Max. thick: >60m.||||||27-NOV-06
15830|Ranford Formation|29813|4|Described|Table 2|||||||||
15830|Ranford Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15830|Ranford Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|31645|6|Mentioned|p4|||See also Table 1||||||
15830|Ranford Formation|32660|5|Briefly described|Table 6|||||||||
15830|Ranford Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
15830|Ranford Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Includes three members: Jarrad Sandstone, Bucket Spring and Ernie Lagoon Members.||||||02-DEC-04
15830|Ranford Formation|32701|4|Described|Table 1|||Adelaidean. Duerdin Group. See p14.||||||27-NOV-06
15830|Ranford Formation|32728|6|Mentioned|Table 7|||See Fig.16||||||
15830|Ranford Formation|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group.  Fissile to massive purple ferruginous siltstone, white siltstone and claystone; minor sandstone. Conformable on Moonlight Valley Tillite. Max. thickness: 40m. Contains "zebra stone" in basal beds.||||||27-APR-05
15830|Ranford Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Purple ferruginous siltstone, white siltstone and claystone; minor sandstone.||||||27-APR-05
15830|Ranford Formation|34230|6|Mentioned|p67|Proterozoic|Proterozoic|Contains zebra rock, a striking red and white banded rock - now submerged in the Ord River reservoir.||||||27-NOV-06
15830|Ranford Formation|36048|6|Mentioned|p381|||||||||
15830|Ranford Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15830|Ranford Formation|36551|6|Mentioned|Table 12|||||||||
15830|Ranford Formation|36888|4|Described|p215|||||||||
15830|Ranford Formation|36898|5|Briefly described|Table 1|||See also p181.||||||27-NOV-06
15830|Ranford Formation|37577|6|Mentioned|p70|||||||||
15830|Ranford Formation|37927|5|Briefly described|p507|||||||||
15830|Ranford Formation|38157|6|Mentioned|Table X|||||||||
15830|Ranford Formation|39210|5|Briefly described|p49|||Age||||||
15830|Ranford Formation|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15830|Ranford Formation|40494|4|Described|p13|||||||||
15830|Ranford Formation|41429|6|Mentioned|p247|||||||||
15830|Ranford Formation|42047|6|Mentioned|p201|||||||||
15830|Ranford Formation|43299|5|Briefly described|Map Legend||Neoproterozoic|Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|43303|5|Briefly described|Map Legend||Neoproterozoic|Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|44140|4|Described|p301 fig 4-7, p302 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. 564 m thick.||Duerdin Group|Jarrad Sandstone Member, Johnny Cake Shale Member.|Overlies Moonlight Valley Tillite. Is overlain unconformably by Mount Forster Sandstone (Albert Edward Group).|Thinly bedded khaki sandstone and fine quartz sandstone.|08-MAR-18
15830|Ranford Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
15830|Ranford Formation|44317|4|Described|Table 3, p.7||Adelaidean|||||||
15830|Ranford Formation|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
15830|Ranford Formation|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean) Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
15830|Ranford Formation|44363|5|Briefly described|p.6,14,20|||(Adelaidean) Of the Duerdin Group.||||||27-NOV-06
15830|Ranford Formation|44364|14|Not recorded|map legend|||||||||
15830|Ranford Formation|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
15830|Ranford Formation|45047|2|Defined|p89|Adelaidean|Adelaidean|See p36.||||||07-NOV-16
15830|Ranford Formation|45112|4|Described|p40|||||||||
15830|Ranford Formation|45140|2|Defined|p13, p59, Appx.p34-35|||Dow and Gemuts (1969). Named after Mount Ranford. Unnamed basin NW of Birrindudu Basin. Mapped as Kearney Beds by Casey and Wells (1964). The type section is [in] Moonlight Valley, Dixon Range sheet area. Forms low strike ridges. Up to 200m thick. No fossils known.||Duerdin Group.||Conformably overlies Redbank Yard Formation. Is overlain unconformably by Mount Forster Sandstone.|Thin-bedded to laminated micaceous siltstone and shale; flaggy, well-sorted, fine-grained sublithic arenite; dolomitic sandstone.|
15830|Ranford Formation|48927|6|Mentioned|Table 1|||Refers Dow and Gemuts (1969).||||||27-NOV-06
15830|Ranford Formation|48938|4|Described|p70|||||||||
15830|Ranford Formation|48943|3|Fully described|p84|||||||||
15830|Ranford Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group.||||||
15830|Ranford Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Includes: Jarrad Sandstone Member. Siltstone and mudstone, greywacke, lithic sandstone, quartz sandstone, dolomitic quartz sandstone and dolomite.||||||05-NOV-04
15830|Ranford Formation|60682|5|Briefly described|p17 Table 4, 19|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Creek Basin.||||||
15830|Ranford Formation|63458|5|Briefly described|p873 Fig.2, p886-889, p897 Fig.19.|Ediacaran|Ediacaran|East Kimberley district.||Unit in Duerdin Group.|Includes Jarrad, and Johnny Cake, Sandstone Members.|Overlies Moonlight Valley Tillite.|Laminated siltstone (Texas/Mabel Downs); sandstone and dolomite (Palm Springs).|12-JUN-15
15830|Ranford Formation|64104|4|Described|p62-63, p66 fig 3, p68 Fig.5, p71-72|Neoproterozoic|Neoproterozoic|In the Purnululu area, parts of this unit have been reinterpreted as belonging to Frank River Sandstone.|||Includes Jarrad Sandstone Member and Johnny Cake Shale Member.|Overlies Moonlight Valley Formation conformably. Is overlain unconformably by Mount Forster Sandstone.|Marine siltstone and sandstone.|
15830|Ranford Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Duerdin Group, Wolfe Creek Basin. Includes Ernie Lagoon, Beasly Knob, Bucket Springs and Jarrad Sandstone Members. Quartz sandstone, siltstone, conglomerate||||||
15830|Ranford Formation|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.|Includes Jarrad Sandstone Member.|Overlies Moonlight Valley Tillite. Is unconformably overlain by Kinevans Sandstone.|Ferruginous siltstone, siltstone and claystone; minor sandstone.|
15830|Ranford Formation|67484|4|Described|p293-299|Ediacaran||East Kimberley. The upper part is a correlative of the Elatina and Nuccaleena Formations. A new Ediacara-type fossil Palaeopascichnus has been identified in the constituent Johnny Cake Shale Member. If correlation with the early Ediacara units in SA is accepted, this represents the earliest identifiable member of the Ediacara biota, and the first Ediacara-type fossil in the Kimberley.||Of the Duerdin Group.|Includes Johnny Cake Shale, Jarrad Sandstone, Members.|Underlain by the Moonlight Valley Tillite. Overlain by the Mount Forster Sandstone. Upper part correlates with Brachina Formation.|Upper part consists of claystone, dolomitic siltstone and fine sandstone.|27-MAY-15
15830|Ranford Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Duerdin Group.|Jarrad Sandstone Member, Johnny Cake Shale Member.|Overlies Moonlight Valley Formation. Is overlain by Mount Forster Sandstone (Albert Edward Group).||
15830|Ranford Formation|68138|5|Briefly described|p153, 155-156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Duerdin Group.||Overlies Moonlight Valley Formation.|Shale, silt/sandstones.|
15830|Ranford Formation|68244|4|Described|p660,668,670|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Nomenclature of Dow and Gemuts 1963, reinterpreted by Corkeron 2008 to be part of Moonlight Valley Formation and Frank River Sandstone.||Unit of Duerdin Group.||Uppermost unit of Duerdin Group. Overlain unconformably by Mount Forster Sandstone. Underlain by Moonlight Valley Formation.||
15830|Ranford Formation|68473|6|Mentioned|p529, 531-532, p534, p547|||||Duerdin Group|Includes the Johnny Cake Shale Member, Jarrad Sandstone Member and the Beasly Knob Member.|Equivalent to the Throssell Shale.||
15830|Ranford Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|Includes Johnny Cake Shale Member, Jarrad Sandstone Member.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone.|04-AUG-15
15830|Ranford Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv.||Duerdin Group|Includes Johnny Cake Shale Member, Jarrad Sandstone Member||Undivided; green to reddish purple siltstone, locally micaceous; minor thin bedded, fine grained quartz sandstone and mudstone.|
15830|Ranford Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Moonlight Valley Tillite and Uniya Formation.||12-JUL-16
15830|Ranford Formation|69442|5|Briefly described|p27:1, 3-4, 6-7|||Wolfe Basin. Widespread in WA, where its thickness reaches 600m. Contains a leached white siltstone with locally-developed red to black Fe-oxide stripes, commercially exploited and marketed as 'zebrastone', mainly in WA.||Duerdin Group.|Ernie Lagoon, Beasly Knob, Bucket Spring, Jarrad Sandstone, Members.|||12-JUL-16
15830|Ranford 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 Duerdin Group.|Includes Jarrad Sandstone Member and Johnny Cake Shale Member.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone|
15830|Ranford Formation|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|Includes Jarrad Sandstone Member, Bucket Spring Member, Beasly Knob Member, Ernie Lagoon Member|||
15830|Ranford Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Duerdin Group|||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone.|
15830|Ranford Formation|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin||Duerdin Group.|Includes Jarrad Sandstone Member.|Shown as overying Moonlight Valley Tillite. May be unconformably overlain by Kinevans Sandstone relationship not clear on map.|Ferruginous siltstone, siltstone and claystone; minor sandstone.|
15830|Ranford 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 Duerdin Group.|Includes Jarrod Sandstone Member, Johnny Cake Shale Member, Moonlight Valley Tillite.||Green to reddish purple siltstone, locally micaceous; minor thin-bedded, fine-grained quartz sandstone and mudstone|
15830|Ranford Formation|73255|4|Described|p532-535, p537-539, p543-546, p548-550|Ediacaran|Ediacaran|Contains Palaeopascichnus and Yangtziramulus fossils. Trough cross-bedded dolomitic sandstone facies deposited in fluvial paleochannels. Interbedded red-green siltstone facies includes gypsum rosettes, desiccation cracks, claystone breccias, planar and wavy bedding, suggested deposition in shallow lacustrine environment. Interbedded red siltstone and sandstone facies with planar/wavy bedding, ripple marks, claystone breccias and Rivularites repertus microbial trace fossil interpreted as fluvial levee, associated with paleochannel facies and eolian reworking. Red sandstone with dolomitic nodules facies represents well drained floodplain environments. Evidence of paleosols comparable with gypsids and calcids. Contains zebra rock in the Johnny Cake Member. Common early burial alterations include gleisation. Specific locations in text include p533 Fig.1, p538 Fig.5, p539 Fig.6 and p541.||Duerdin Group|Johnny Cake Member, Jarrad Member|Conformably overlies the Moonlight Valley Tillite, disconformably underlies the Kinevans Sandstone, and Mount Forster Sandstone, underlies the Albert Edward Group.|Dolomitic sandstones in lower part. Includes trough cross-bedded dolomitic sandstone, finely interbedded red-green siltstone, medium to coarse sandstone with interbedded fine grained sandstone and siltstone, red sandstones with dolomitic nodules.|
15929|Red Bull Member|24000|3|Fully described|p349|Devonian|Devonian|Of Pillara Formation.  Max. thickness: 270m.  Geological Province: Canning Basin.||||||
15929|Red Bull Member|31870|6|Mentioned|p113|||||||||
15929|Red Bull Member|40837|6|Mentioned|p264|||||||||
15929|Red Bull Member|41215|6|Mentioned|Fig.17|||||||||
15929|Red Bull Member|45153|5|Briefly described|App.3-51|||||||||
15947|Red Lake Ophiolites|29784|6|Mentioned|Table 1|||||||||
15947|Red Lake Ophiolites|30900|6|Mentioned|p67|||On Table 1||||||
15947|Red Lake Ophiolites|31042|6|Mentioned|Fig. 2|||||||||
15947|Red Lake Ophiolites|34324|6|Mentioned|p122|||Table||||||
15947|Red Lake Ophiolites|37373|6|Mentioned|Table 2.I|||||||||
15947|Red Lake Ophiolites|42892|5|Briefly described|Table 4|||||||||
15947|Red Lake Ophiolites|73391|6|Mentioned|Appendices.|||Glikson (1971). Regional stratigraphic correlation chart of other workers.|||||Basalt, andesite, dolerite, meta pyroxenite.|
15980|Redbank Yard Formation|22496|3|Fully described|p10||Neoproterozoic|Of the Duerdin Group.  Concordant on the Illjarra Sandstone; conformably overlain by the Ranford Formation.  Max. thickness: 1000m.  Geological Province:  Wolfe Basin.||||||12-AUG-04
15980|Redbank Yard Formation|22777|5|Briefly described|Map|||Duerdin Group, Wolfe Basin||||||
15980|Redbank Yard Formation|23621|4|Described|p33|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Duerdin Group. Overlying unit Ranford Formation. Underlying unit Illjarra Sandstone. Wolfe Basin. Max. thickness: 1000 m.||||||
15980|Redbank Yard Formation|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
15980|Redbank Yard Formation|29813|4|Described|Table 2|||||||||
15980|Redbank Yard Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15980|Redbank Yard Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15980|Redbank Yard Formation|37927|6|Mentioned|p508|||||||||
15980|Redbank Yard Formation|43303|5|Briefly described|Map Legend||Neoproterozoic|of Duerdin Group.||||||
15980|Redbank Yard Formation|45140|2|Defined|p13, p57, p59, Appx.p34|||Blake et al. (1977), Blake and Yeates (1977). Named after Redbank Yard on Wolf Creek; the type section is 16km WSW of that location, at 19deg 07'S, 127deg 36'30"E. A unit in an unnamed basin NW of the Birrindudu Basin. Mapped as part of Kearney Beds by Casey and Wells (1964). Forms a group of isolated strike ridges. Maximum known thickness of 330m at the type section.||Duerdin Group.||Overlies Wade Creek Sandstone, probably unconformably. Is overlain by Ranford Formation, probably conformably. Lateral equivalent of Moonlight Valley Tillite.|Conglomerate, medium-bedded sublithic arenite, minor dolomite.|
15980|Redbank Yard Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|||Polymictic conglomerate, cross-bedded, medium to coarse and commonly pebbly sublithic sandstone, minor dolomite.|04-AUG-15
15980|Redbank Yard Formation|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|||Duerdin Group|||Polymictic conglomerate, cross bedded medium to coarse and commonly pebbly sublithic sandstone, minor dolomite.|
15980|Redbank Yard 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 Duerdin Group.|||Polymictic conglomerate, cross-bedded, medium to coarse and commonly pebbly sublithic sandstone, minor dolomite|
15980|Redbank Yard Formation|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Polymictic conglomerate, cross bedded, medium to coarse and commonly pebbly sublithic sandstone and minor dolomite.|
15980|Redbank Yard Formation|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.|||Polymictic conglomerate, cross-bedded, medium to coarse and commonly pebbly sublithic sandstone, minor dolomite|
15983|Redcliff Pound Group|23621|6|Mentioned|p32|||||||||
15983|Redcliff Pound Group|24173|6|Mentioned|p24|Neoproterozoic|Neoproterozoic|Probable correlative of Ruby Plains Group (in the Billiluna 1:250,000 sheet area||||||
15983|Redcliff Pound Group|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29807|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|29809|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29812|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|29813|4|Described|Table 2|||||||||
15983|Redcliff Pound Group|29817|6|Mentioned|p7|||||||||
15983|Redcliff Pound Group|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15983|Redcliff Pound Group|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15983|Redcliff Pound Group|31360|6|Mentioned|Table 1|||||||||
15983|Redcliff Pound Group|31362|6|Mentioned|p8|||||||||
15983|Redcliff Pound Group|32660|6|Mentioned|p243|||||||||
15983|Redcliff Pound Group|33102|6|Mentioned|Fig.2|||||||||
15983|Redcliff Pound Group|33965|6|Mentioned|p7|||||||||
15983|Redcliff Pound Group|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|35222|6|Mentioned|p10|||||||||
15983|Redcliff Pound Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15983|Redcliff Pound Group|36551|6|Mentioned|Table 12|||||||||
15983|Redcliff Pound Group|37299|6|Mentioned|Fig.1|||Misspelling? [No. Redcliffe Pound Group is the misspelling. CEBApr95]||||||
15983|Redcliff Pound Group|37462|6|Mentioned|Table 4.V|||||||||
15983|Redcliff Pound Group|42504|5|Briefly described|Table 4 P73|||||||||
15983|Redcliff Pound Group|43175|5|Briefly described|p6||Proterozoic|||||||
15983|Redcliff Pound Group|43631|6|Mentioned|p20|||||||||
15983|Redcliff Pound Group|45112|5|Briefly described|p29|||||||||
15983|Redcliff Pound Group|45140|2|Defined|p12-14, p17-18, p22, p26, p28, p39-40|Neoproterozoic|Neoproterozoic|See also p42-46, p48, p51-53, p56-60, p63-64, p66-67, p74-75, Appx.p23. Hodgson (1976); Blake and Yeates (1977). Named after Redcliff Pound. Birrindudu Basin. Generally gently dipping. Maximum exposed thickness is c.1300m; true thickness may be well over 2000m. No mineralisation yet been found. Younger than 1076 +/- 50 Ma (age of migmatite underlying Heavitree Quartzite). Is overlain by Hidden Basin Beds, and unconformably by Lucas Formation, Hazlett Beds and Knobby Sandstone.|||Lewis Range, Muriel Range, Munyu, Erica Sandstones; Murraba Formation.|Unconformably overlies Killi Killi and Mount Charles Beds, Arunta Complex, Birrindudu Group. Correlated with Heavitree Quartzite, Bitter Springs Formation, Vaughan Springs Quartzite, Limbunya Group.||
15983|Redcliff Pound Group|46788|6|Mentioned|p8|||||||||
15983|Redcliff Pound Group|46864|4|Described|p38|||||||||
15983|Redcliff Pound Group|50315|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes: Muriel Range Sandstone.  Age: <800Ma.||||||09-JUN-04
15983|Redcliff Pound Group|50374|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Muriel Range Sandstone||||||
15983|Redcliff Pound Group|50376|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone.||||||22-JUN-04
15983|Redcliff Pound Group|60676|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes Muriel Range Sandstone. Sublithic arenite, quartz arenite, minor siltstone, shale, conglomerate, arkose, breccia.||||||19-JAN-05
15983|Redcliff Pound Group|61861|6|Mentioned|p4, p23, Map 1|Paleozoic|Neoproterozoic|Neoproterozoic?|||Includes Muriel Range Sandstone.|||
15983|Redcliff Pound Group|62580|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|Part of a thick sequence of predominantly sublithic and quartz arenite in the Tanami region.||||||07-FEB-11
15983|Redcliff Pound Group|62628|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||15-AUG-06
15983|Redcliff Pound Group|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||23-DEC-09
15983|Redcliff Pound Group|62633|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Murraba Basin.||||||
15983|Redcliff Pound Group|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.||||||09-DEC-08
15983|Redcliff Pound Group|64635|6|Mentioned|p2 Fig.1|||||||||
15983|Redcliff Pound Group|64675|6|Mentioned|p10, Fig.21, Map 1|||||||||19-MAR-14
15983|Redcliff Pound Group|64724|5|Briefly described|p49 Fig. 7||Cryogenian|Age very poorly constrained. May be as young as Ediacaran||||||
15983|Redcliff Pound Group|64733|6|Mentioned|p169 Fig.1|Neoproterozoic|Neoproterozoic|||||||
15983|Redcliff Pound Group|65074|6|Mentioned|p350-351, p353, p356-357 Tb.4-12|Neoproterozoic|Neoproterozoic|See also p358, p360, p362. Of North/Centre Birrindudu Basin. Over 2 km thick. Deposition from c.1000 Ma.|||Lewis Range, Muriel Range, Munyu, Erica Sandstones; Murraba Formation.|Is overlain unconformably by Lucas Formation.||
15983|Redcliff Pound Group|65323|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not present on map; Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||02-FEB-10
15983|Redcliff Pound Group|65324|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone; Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65326|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65327|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65328|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65332|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Murraba Basin. Includes Munyu Sandstone||||||02-FEB-10
15983|Redcliff Pound Group|65349|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone; Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65350|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65351|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||
15983|Redcliff Pound Group|65352|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone||||||12-APR-10
15983|Redcliff Pound Group|65353|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone.||||||11-DEC-12
15983|Redcliff Pound Group|65354|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone;||||||12-APR-10
15983|Redcliff Pound Group|65355|5|Briefly described|cross section|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone. Age given as 800 Ma?||||||10-DEC-12
15983|Redcliff Pound Group|65356|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Not shown on map; Includes the Muriel Range Sandstone||||||12-APR-10
15983|Redcliff Pound Group|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Includes Erica and Munyu Sandstones and Murraba Formation.|Unconformably overlies Reynolds Range Group.||19-OCT-11
15983|Redcliff Pound Group|67168|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||Includes Muriel Range Sandstone.|Unconformably overlies Tanami Group, Inningarra Suite and Pargee Sandstone. Is unconformably overlain by Antrim Plateau Volcanics.||
15983|Redcliff Pound Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Neoproterozoic|Neoproterozoic|Murraba Basin. See also 500k_interpgeop_lut.csv and GEOCHRON. Is mysteriously referred to as Redcliffe Plain Group, Redcliff Plain Group and Redcliff Pound Group in Geochronology dataset 743, which locates  it in the Birrindudu Basin.|||||Undivided; quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert and glauconitic sandstone.|
15983|Redcliff Pound Group|68733|6|Mentioned|p176 Fig.1, p188|||Murraba Basin.|||Includes the Munya and Lewis Range Sandstones (basal units).|||05-DEC-17
15983|Redcliff Pound Group|68994|4|Described|p20|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Manyu Sandstone at base|Unconformably overlies Aileron Province rocks.||
15983|Redcliff Pound Group|69003|6|Mentioned|p5, p61|||Murraba Basin, Granites-Tanami Orogen.||||||
15983|Redcliff Pound Group|69031|6|Mentioned|p4, p6 Fig.4, p8|||Murraba Basin.|||Munyu Sandstone.|||
15983|Redcliff Pound Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Murraba Basin|||Includes Lewis Range Sandstone.||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|04-AUG-15
15983|Redcliff Pound Group|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Munyu, Erica Sandstones; Murraba Formation.|||
15983|Redcliff Pound Group|69432|5|Briefly described|p17:2, 13|Neoproterozoic|Neoproterozoic|Murraba Basin. Generally shallow-dipping.||||Overlies Birrindudu Group.||12-JUL-16
15983|Redcliff Pound Group|69437|5|Briefly described|p22:6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.|||Munyu, Erica Sandstones; Murraba Formation.||Almost exclusively siliciclastic sedimentary rocks.|12-JUL-16
15983|Redcliff Pound Group|69440|5|Briefly described|p25:1|||Murraba Basin. Siliciclastic sediments. Probably over 2000m thick.|||Munyu, Erica Sandstones; Murraba Formation.|||12-JUL-16
15983|Redcliff Pound Group|69453|6|Mentioned|p37:1|||Murraba Basin.||||Is inferred to be overlain unconformably by Lucas Formation.||12-JUL-16
15983|Redcliff Pound Group|69508|5|Briefly described|Map legend.|Neoproterozoic|Paleoproterozoic|Murraba Basin.|||Munya Sandstone.|||
15983|Redcliff Pound Group|69587|4|Described|GEOL_LUT_CSV files + geochron files|Cryogenian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|830-810 Ma (inferred)||Includes Lewis Range Sandstone.||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone|
15983|Redcliff Pound Group|69634|4|Described|GEOL_LUT_CSV files||Neoproterozoic|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|830-810 Ma (Inferred)||Includes Lewis Range Sandstone.||Undivided; quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone|
15983|Redcliff Pound Group|69673|6|Mentioned|p187|||More than 2000m thick.|||Includes Munyu Sandstone, Muriel Range Sandstone, Murraba Formation, Erica Sandstone|||
15983|Redcliff Pound Group|70129|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|||Lewis Range Sandstone, Murraba Formation.|||
15983|Redcliff Pound Group|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|||Lewis Range, Erica Sandstones; Murraba Formation.||Dominantly sandstones; also conglomerate, siltstone and mudstone; minor limestone.|
15983|Redcliff Pound Group|70141|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.||Lewis Range Sandstone.|Overlies Birrindudu Group.||
15983|Redcliff Pound Group|70142|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.|830-810 Ma.||Lewis Range Sandstone.|||
15983|Redcliff Pound Group|70143|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin. Unclear if age range refers to the Group or just the Lewis Range Sandstone.|830-810 Ma.||Lewis Range Sandstone.|||
15983|Redcliff Pound Group|70154|4|Described|100k_interpgeop_lut.csv|Cryogenian|Neoproterozoic|See also 500k_interpgeop_lut.csv.|810-1000 Ma||Includes Lewis Range Sandstone||Quartz sandstone and wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|
15983|Redcliff Pound Group|70826|6|Mentioned|p5 tbl 2|||Centralian Superbasin.||||||20-APR-20
15983|Redcliff Pound Group|70851|6|Mentioned|p19|||||||||
15983|Redcliff Pound Group|70852|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.|||Muriel Range Sandstone.|||
15983|Redcliff Pound Group|71080|1|Redefined|p1, p4, 6, 20, 27-28,  29, 31,32  36-38|Cambrian|Ediacaran|Murraba Basin. Previously believed to be Tonian.The term was first used by Blake et al (1973) and subsequently defined in Blake et al (1979). Originally this group contained the Lewis Range, Muriel Range and Munyu sandstone overlain by Murraba Formation and the Erica Sandstone. Outcrop is restricted to eastern STANSMORE and southeastern LUCAS 1;250k map sheets. Is expressed in outcrop as low strike ridges and strike valleys. This group is gently to tightly folded and faulted but not metamorphosed. At least 2000 m thick, as originally defined. Now restricted to Redcliff Pound area - c 1500 m thick, and supersequences 3 & 4 of the Centralian Superbasin.  Age inferred for regional correlations. Hosts Arumberia and probable tubular body fossils. Distinguishing and identifying features are discussed.|||Includes Murraba Formation, Erica Sandstone.|Unconformable over mostly concealed, unnamed units (likely supersequence 1-2 ). Unconformably overlain by Paleozoic outliers of Canning Basin in WA and Antrim Plateau Volcanics in NT.|Murraba Formation: Sandstone, siltstone, and minor carbonate and conglomerate deposited in shallow marine to deltaic environments. Erica Sandstone: predominantly sandstone deposited in deltaic, fluvial and eolian environments.|04-FEB-19
15983|Redcliff Pound Group|71267|4|Described|GEOL_LUT_CSV files|Cambrian|Cryogenian|Of Murraba Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|650-510 Ma (inferred)||Includes Erica Sandstone, Lewis Range Sandstone.||Abundantly cross bedded and rippled medium grained quartz sandstone, minor sublithic sandstone, shale, siltstone, conglomerate, arkose, breccia; some convolute lamination and disturbed cross beds|
15983|Redcliff Pound Group|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cryogenian|Murraba Basin.|||||Quartz sandstone; minor conglomerate, siltstone, shale, carbonate and glauconitic sandstone.|
15983|Redcliff Pound Group|73445|5|Briefly described|p3, 6-8, 10, 12, 23-24, 29, 34-35|Cambrian|Neoproterozoic|See also p37-38, 41-47, 56, 65-118. Murraba Basin. Over 2,000m thick. Multi-element spider diagram. Regolith chemistry tabulated.|||Munyu, Lewis Range, Muriel Range, Erica Sandstones; Murraba Formation.|Unconformably overlies the Killi Killi Formation. Correlated with Heavitree Quartzite.|Sandstone, wacke; minor conglomerate, siltstone, shale, limestone, dolomite, chert, and glauconitic sandstone.|
15999|Reef Complex|22753|5|Briefly described|Fig.3 p585|Devonian|Devonian|||||||
15999|Reef Complex|22767|5|Briefly described|Table3 P18, P11|Late Devonian|Middle Devonian|Informal name for possible equivalents of Pillara Limestone, Gogo Formation, Nullara Limestone.||||||
15999|Reef Complex|30895|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
15999|Reef Complex|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Devonian|Devonian|Offshore Canning Basin.|||Includes Pillara Limestone.|Is overlain by Fairfield Group.||01-MAY-19
15999|Reef Complex|73117|6|Mentioned|p3|Famennian|Frasnian|Canning Basin. Contemporaneous with extensional movements.||||Disconformably overlain by Fairfield Group including Gumhole Formation.|Carbonates.|
16001|Regal Formation|22471|5|Briefly described|25|Archean|Archean|Geol province Pilbara||||||07-NOV-08
16001|Regal Formation|23484|4|Described|p10 table 2|Archean|Archean|Of Roebourne Group. Maximum thickness: ~2000m.||||||07-NOV-08
16001|Regal Formation|23783|5|Briefly described|p37 Tb. 3|Archean|Archean|||||||07-NOV-08
16001|Regal Formation|23784|5|Briefly described|p10|Archean|Archean|Of Roebourne Group.||||||07-NOV-08
16001|Regal Formation|23789|5|Briefly described|p9 Tb. 2|Archean|Archean|Of the Roebourne Group.  Max. thickness: 2000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
16001|Regal Formation|23793|4|Described|p15|Archean|Archean|Of Roebourne Group. See also page 12 table 2.  Age: 3018 +/- 2 Ma||||||07-NOV-08
16001|Regal Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Roebourne Group. Geological Province: Pilbara Craton.||||||07-NOV-08
16001|Regal Formation|23813|5|Briefly described|p101|Archean|Archean|Of the Roebourne Group.  Age: 3.27-3.26Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
16001|Regal Formation|23936|4|Described|Tb.1|Archean|Archean|Age: 3.27-3.26 Ga. Geological Province: Pilbara Craton. Of the Roebourne Group. Underlain by Nickol River Formation.||||||07-NOV-08
16001|Regal Formation|24023|5|Briefly described|p7 fig. 4|Archean|Archean|Of Roebourne Group. Maximum thickness: 2000m.||||||07-NOV-08
16001|Regal Formation|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Roebourne Group. Geological Province: Pilbara Craton||||||07-NOV-08
16001|Regal Formation|24184|4|Described|p711 Tb.1, p709|Archean|Archean|Of the Roebourne Group. Underlain by Nickol River Formation. Geological Province: Pilbara Craton. Max Thickness: 2000m. Age: >3018 +/- 2Ma. Assignment to the Roebourne Group (Hickman 1997) is questionnable pending precise dating||||||07-NOV-08
16001|Regal Formation|24541|1|Redefined|p11 Tb.2, p20-21|Archean|Archean|Geological Province: West Pilbara Granite-Greenstone Terrane. Age: minimum 3018 Ma. Maximum Thickness: 2000m. Overlies the Nickol River Formation. Overlain by the Cleaverville Formation. Previously assigned to the Roebourne Group.||||||23-DEC-09
16001|Regal Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Roebourne Group (Pilbara Supergroup).  Age: >3125Ma.  Massive and pillow basalt with local basal peridotitic komatiite; minor chert.||||||07-NOV-08
16001|Regal Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Roebourne Group. Consists of komatiites, basalt and minor chert. Underlies Cleaverville Formation in West Pilbara. Thickness: 2km. Geological Province: Pilbara Craton. See also p76.||||||07-FEB-11
16001|Regal Formation|30766|6|Mentioned|p5|||Refers Ryan & Friewaldt (1964).||||||
16001|Regal Formation|30882|4|Described|p50|||Re stratigraphy.||||||01-AUG-07
16001|Regal Formation|31853|6|Mentioned|Table 9|||Refers Ryan (1964,1965)||||||
16001|Regal Formation|36874|6|Mentioned|p84|||||||||
16001|Regal Formation|39697|6|Mentioned|p15|||||||||
16001|Regal Formation|42231|6|Mentioned|p334|||||||||
16001|Regal Formation|44477|5|Briefly described|p.6|||SF/50-6.||||||
16001|Regal Formation|44478|14|Not recorded|map legend||Archean|||||||07-NOV-08
16001|Regal Formation|44501|14|Not recorded|p.7, table 2, map||Archean|(ref. to Ryan and Kriewaldt 1964). (F/50-7).||||||07-NOV-08
16001|Regal Formation|44502|14|Not recorded|map legend||Archean|||||||07-NOV-08
16001|Regal Formation|44536|14|Not recorded|map legend||Archean|||||||07-NOV-08
16001|Regal Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Roebourne Group. Geological Province: Pilbara Craton.||||||07-NOV-08
16001|Regal Formation|50430|4|Described|p153||Archean|>3160 Ma. Ultramafic to mafic volcanics. Here removed from Roebourne Group and placed in Cleaverville Formation. Has tectonic contact with Nickol River Formation, and is disconformably overlain by Cleaverville Formation.||||||07-NOV-08
16001|Regal Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Unconformably overlain by Cleaverville Formation.  Age: ~3.2Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
16001|Regal Formation|63441|5|Briefly described|p5 Tb.1, p24|Archean|Archean|Of Whundo Group (Pilbara Supergroup). Age: older than c.3.2Ga Orpheus Supersuite felsic sills. Overlain by Cleaverville Fm.  In structural contact with Ruth Well and Nickol River Formations. Geological province: West Pilbara Superterrane.||||||07-APR-14
16001|Regal Formation|63518|5|Briefly described|p752|Archean|Archean|Geological Province: Pilbara Craton. Basaltic greenstones.||||||07-NOV-08
16001|Regal Formation|63538|4|Described|p2 Fig. 1, p5, p22, p29, p30, p31, p35|Archean|Archean|Underlain by Roebourne Group and Karratha Granodiorite. Geological Province: Pilbara Craton. Dominantly amphibolite facies metabasalt.||||||07-FEB-11
16001|Regal Formation|63649|5|Briefly described|p200 Fig. 1|Archean|Archean|Geological Province: West Pilbara Terrane/ Regal Terrane. Granitic rocks.||||||07-FEB-11
16001|Regal Formation|64174|5|Briefly described|Map legend|Archean|Archean|Geological province: Regal Terrane. Massive and pillowed basalt, with local komatiitic peridote; minor chert; metamorphosed.||||||07-NOV-08
16001|Regal Formation|64580|4|Described|map legend||Mesoarchean|Massive and pillowed basalt, with local komatiitic peridotite; minor chert; metamorphosed.||||||09-DEC-08
16001|Regal Formation|64632|6|Mentioned|p201 Fig.1, p202, 207|||Regal Terrane, West Pilbara Superterrane. ~3.5km thick|||||mid-ocean ridge-like basalts|
16001|Regal Formation|66118|5|Briefly described|p146 Fig.1, p151, p153-154, p158-159|||Pilbara Craton. West Pilbara Superterrane. Regal Terrane. See also Regal Basalt in this paper.|c. 3200 Ma|||Tectonically overlies rocks of Karratha Terrane (3270 Ma). Is stratigraphically overlain by Cleaverville Formation.|Dominantly composed of lower amphibolite-facies metabasalt, but includes thick flows of Al-depleted olivine spinifex-textured komatiite at base of formation.|
16001|Regal Formation|66217|5|Briefly described|p9, p38.|Archean|Archean|Regal Terrane. Possibly formed as a result of rifting during the Soanesville Event at 3200-3165 Ma.|c.3.2 Ga.||||MORB basalts.|
16001|Regal Formation|67201|4|Described|p3, p7, p10, p13-17, see comments|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane, Regal Terrane. In informal Cleaverville succession. Thickness: 2-3 km. Age: approximate depositional age 3200 Ma (Nd isotopic data), and 3195 Ma (U-Pb zircon age from thin felsic tuff unit in Dixon Island Formation underlying Regal Formation on Dixon Island). Min age: c. 3160 Ma (age of thermal event that metamorphosed formation). Lithological composition and geochemistry (MORB-like) are suggestive of oceanic crust. The Formation's basalts show no geochemical evidence of crustal contamination. Depositional environment: mostly deep-water oceanic. Slices of mafic and ultramafic schist from this unit occur within upper part of underlying Nickol River Formation. Is intruded by dacite sills of Orpheus Supersuite. Page location continued: p20-21, p25-27, p37, p41-44, p67-69.|c. 3200 Ma|||Overlies Dixon Island Formation. Underlies Gorge Creek Group (Cleaverville Formation, "Sixty-six Hills Member") nonconformably. Is faulted against Whundo Group and Nickol River Formation.|Massive and pillowed basalt, with local basal komatiitic peridotite; minor chert, BIF, and shale. Includes strongly foliated amphibolite-chlorite schist. Metamorphosed to amphibolite or upper greenschist facies.|25-NOV-16
16001|Regal Formation|67269|6|Mentioned|p2 Fig.1|Paleoarchean|Paleoarchean|Regal Terrane, W. Pilbara Superterrane.||||||
16001|Regal Formation|68035|4|Described|p289, 293, p285 Fig 2, p290 Fig 5|Mesoarchean|Mesoarchean|Remnant of Regal Terrane oceanic crust. 2-3 km thick. Interpreted to have been obducted onto Karratha Terrane between 3160 and 3070 Ma. May include microbial mats.|3.19 Ga|||Overlies Karratha Terrane and Nickol River Formation.|Metamorphosed pillow basalt, local basal komatiitic peridotite, and rare chert.|
16001|Regal Formation|68284|6|Mentioned|p2|||West Pilbara Superterrane.||||||
16001|Regal Formation|68574|5|Briefly described|p4-5|||Ryan and Kriewaldt (1964); Hickman (1997). Cleaverville Beach area, NW Pilbara Craton.||||Is overlain by Dixon Island Formation, Cleaverville Formation.||
16001|Regal 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.||Unit of Roebourne Group.|||Massive and pillowed basalt, with local komatiitic peridotite; minor chert; metamorphosed|
16001|Regal Formation|69301|4|Described|p3 Fig.1, p5-p6, p9 Tb.1, p13-14|||Pilbara Craton. West Pilbara Superterrane. Regal Terrane. Of Cleaverville succession (informal stratigraphic name). Thickness: 2-3 km. Sholl Shear zone above, Regal Thrust zone below. Age: Nd isotopic data (Smithies et al. 2007a) interpreted as approximate depositional age (Van Kranendonk et al. 2007b). Interpreted as a slice of oceanic crust (ophiolite).|3.20 Ga Nd isotopic data, see comments|||Overlies Dixon Island Formation and Nickol River Formation. Is unconformably overlain (without angular discordance) by Gorge Creek Group.|Mafic volcanic rocks. Sequence of metamorphosed pillow basalt, local basal komatiitic peridotite, with rare chert.|
16001|Regal Formation|69740|5|Briefly described|p651, 663, 673, 676|Mesoarchean|Mesoarchean|Suprasubduction zone-type  or MORB-type ophiolite.|3.2 Ga.||||Pillowed and massive lava, hyaloclastite, dykes, BIF/bedded chert, volcaniclastics.|
16001|Regal Formation|70022|6|Mentioned|p114-115|||Regal Terrane, West Pilbara Superterrane.|3200 Ma.|||||
16001|Regal Formation|70775|4|Described|iv, p1, p6, p10, p12-p13, p15|Mesoarchean|Paleoarchean|Regal Terrane. Interpreted to have been deposited in relatively small extensional basin between continental microplates. This unit is overlain by (and in places, equivalent to) the Port Robinson Basalt. Unconformably overlain by the Cleaverville Formation.See also p19-p22, p25 tbl 4, p26, p28-p31, p33, p41, p44 fig 27, p47-p48, p50, p57, p72-p73, p99.|c. 3200 Ma|||Overlies (or is faulted against) the Nickol River Formation. Overlies the Dixon Island Formation. Faulted against the Soanesville Group.|Massive and pillowed tholeiitic basalt, dolerite and gabbro sills with minor komatiite and komatiitic basalt.|
16001|Regal Formation|70826|6|Mentioned|p8|Mesoarchean|Mesoarchean|West Pilbara Superterrane.||||||
16001|Regal Formation|71349|6|Mentioned|p738|||Resulted from c.3.2 Ga rifting of the Pilbara.|||||Basalts.|
16001|Regal Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Central Pilbara Basin.|||||Massive and pillowed basalt, with local komatiitic peridotite; minor chert; metamorphosed.|
16001|Regal Formation|72251|5|Briefly described|p52,54|Paleoarchean|Paleoarchean|Geological province: Regal Terrane, West Pilbara Superterrane, Pilbara Craton.|3200 Ma|||Overlain by Nallana Formation. Thrust over Nicol River Formation.||
16001|Regal Formation|72668|5|Briefly described|p3-4, p8, p11-13, p25, p28|||Regal Terrane of the West Pilbara Superterrane. 3.5km thick.|c. 3200 Ma||||MORB-like basalts.|13-JAN-22
16050|Revolver Creek Formation|22547|3|Fully described|p22||Orosirian|Revolver Creek Basin. 1800 Ma. 1200 m thick. Overlies Lamboo Complex, overlain by Hensman Sandstone||||||
16050|Revolver Creek Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
16050|Revolver Creek Formation|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16050|Revolver Creek Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone and mudstone, and dolerite, basalt and basaltic breccia; minor conglomerate.  Geological Province:  Revolver Creek Basin.||||||07-NOV-08
16050|Revolver Creek Formation|30097|6|Mentioned|Fig.54|||Also Tables 23,24||||||
16050|Revolver Creek Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16050|Revolver Creek Formation|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16050|Revolver Creek Formation|32660|5|Briefly described|Table 3|||||||||
16050|Revolver Creek Formation|32728|5|Briefly described|p38|||||||||
16050|Revolver Creek Formation|36551|6|Mentioned|Table 10|||||||||
16050|Revolver Creek Formation|36885|4|Described|p176|||||||||
16050|Revolver Creek Formation|36902|6|Mentioned|p11|||||||||
16050|Revolver Creek Formation|37462|4|Described|Table4.III|||||||||
16050|Revolver Creek Formation|38482|6|Mentioned|Table 1|||||||||
16050|Revolver Creek Formation|38988|6|Mentioned|Fig.4|||||||||
16050|Revolver Creek Formation|41158|5|Briefly described|p39|||||||||
16050|Revolver Creek Formation|41703|6|Mentioned|p232|||||||||
16050|Revolver Creek Formation|42191|5|Briefly described|p439|||See also Fig.7||||||
16050|Revolver Creek Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
16050|Revolver Creek Formation|44140|5|Briefly described|p293-294, p296, p298 fig 4-5, p299|Paleoproterozoic|Paleoproterozoic|Ungrouped. Basic volcanics overlain by marine sediments. Up to 1200 m thick.||||Unconformably overlies Whitewater Volcanics. Is overlain unconformably by Carr Boyd Group. Correlated with Kimberley Group.|Amygdaloidal basalt, quartz sandstone, siltstone, arkose.|08-MAR-18
16050|Revolver Creek Formation|44155|6|Mentioned|p250 Tb.3-10, p254 Fig.3-40|||||||Overlain by Hensman Sandstone.||
16050|Revolver Creek Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
16050|Revolver Creek Formation|44363|5|Briefly described|p.6,7,9,11,12,17,24|||(Carpentarian).||||||
16050|Revolver Creek Formation|44364|14|Not recorded|map legend||Proterozoic|||||||
16050|Revolver Creek Formation|45047|4|Described|p28|||Carpentarian. See p29.||||||27-NOV-08
16050|Revolver Creek Formation|63866|5|Briefly described|p133|||Western Zone, Halls Creek Orogen.||||Possibly equivalent to the Kimberley Group.|Arkose, siltstone, conglomerate and basaltic rocks.|
16050|Revolver Creek Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, and mudstone, and dolerite, basalt, and basaltic breccia; minor conglomerate.||||||09-DEC-08
16050|Revolver Creek Formation|68078|6|Mentioned|p23|||Broadly similar to lower Kimberley Group, may be broadly coeval.||||||
16050|Revolver Creek Formation|69003|6|Mentioned|p5, p19, p42|||Lamboo Province, Halls Creek Orogen. With the Carr Boyd Group, hosts the diamondiferous Argyle lamproite intrusion.||||||
16050|Revolver Creek Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Revolver Creek Basin|||Includes unnamed member||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, and siltstone and mudstone; dolerite, basalt, and basaltic breccia; minor conglomerate.|04-AUG-15
16050|Revolver Creek Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|||||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, and siltstone and mudstone; dolerite, basalt, and basaltic breccia; minor conglomerate.|
16050|Revolver Creek Formation|69585|6|Mentioned|p4-5|Statherian|Statherian|||||Probable equivalent of the Kimberley Group.||13-JUN-17
16050|Revolver Creek Formation|69597|6|Mentioned|p5 fig 2b|||||||||
16050|Revolver Creek Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Revolver Creek Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|2500-1600 Ma (Inferred)||||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, and siltstone and mudstone; dolerite, basalt, and basaltic breccia; minor conglomerate, dolerite, basalt, and basaltic breccia|
16050|Revolver Creek Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1600-2500 Ma||||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, siltstone and mudstone, dolerite, basalt, and basaltic breccia; minor conglomerate.|
16050|Revolver Creek Formation|70731|6|Mentioned|p268|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
16050|Revolver Creek Formation|70812|5|Briefly described|p6, p23|Statherian|Orosirian|Central and Eastern zones of the Halls Creek Orogen, Lamboo Province.|c. 1800-1750 Ma|||||
16050|Revolver Creek Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Revolver Creek 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.|2500-1600 Ma (inferred)||||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, and siltstone and mudstone; dolerite, basalt, and basaltic breccia; minor conglomerate|
16050|Revolver Creek Formation|71397|6|Mentioned|p5|Proterozoic|Proterozoic|Geological province: Central and Eastern zones, Lamboo Province, Halls Creek Orogen.||||||
16050|Revolver Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Revolver Creek Basin.|||||Quartz sandstone, lithic quartz sandstone, feldspathic quartz sandstone, and siltstone and mudstone; dolerite, basalt, and basaltic breccia; minor conglomerate.|
16072|Rice Hill lamproite|41158|5|Briefly described|p203|||Mention P204||||||
16074|Richenda Microgranodiorite|23722|6|Mentioned|p12|||||||||
16074|Richenda Microgranodiorite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
16074|Richenda Microgranodiorite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16074|Richenda Microgranodiorite|30533|4|Described|p12|||On Table 1||||||
16074|Richenda Microgranodiorite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16074|Richenda Microgranodiorite|32728|6|Mentioned|p28|||||||||
16074|Richenda Microgranodiorite|36885|4|Described|p170|||||||||
16074|Richenda Microgranodiorite|42710|5|Briefly described|map legend|Proterozoic||||||||
16074|Richenda Microgranodiorite|42811|5|Briefly described|p10|||||||||
16074|Richenda Microgranodiorite|42814|6|Mentioned|p9|||||||||
16074|Richenda Microgranodiorite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
16074|Richenda Microgranodiorite|44155|6|Mentioned|p240|||Undeformed and discordant; associated rhyolite dykes.||Hooper Complex.||||
16074|Richenda Microgranodiorite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Used interchangeably with Richenga Granite.||||||07-NOV-08
16074|Richenda Microgranodiorite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1858 Ma|Paperbark Supersuite||||
16074|Richenda Microgranodiorite|69099|5|Briefly described|ga_geochron.csv|Paleoproterozoic|Paleoproterozoic|King Leopold Inlier. Data migrated from OZCHRON1. Igneous crystallisation age.|1858 +/-5 Ma SHRIMP|||||
16074|Richenda Microgranodiorite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic||1858 Ma|||||
16074|Richenda Microgranodiorite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|c.1858 Ma (Tyler et al., 1999).|Paperbark Supersuite.|||Foliated, medium- to fine-grained metagranodiorite and metatonalite.|
16074|Richenda Microgranodiorite|70154|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1858 Ma|Paperbark Supersuite|||Foliated, medium- to fine-grained metagranodiorite and metatonalite.|
16074|Richenda Microgranodiorite|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_geologyp_lut.csv and geochron files.|1858+\-5 Ma (isotopic)|Unit of Paperbark Supersuite.||Intrudes into Marboo Formation.|Foliated, medium- to fine-grained metagranodiorite and metatonalite|
16091|Ridge Hill Sandstone|23816|6|Mentioned|p256|||Max. thickness: 15 m.||||||
16091|Ridge Hill Sandstone|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
16091|Ridge Hill Sandstone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Consists of ferruginous sandstone with a thin basal conglomerate overlying Precambrian crystalline rocks and capped by laterite. Geological Province: Perth Basin.||||||24-NOV-09
16091|Ridge Hill Sandstone|30217|5|Briefly described|p21|||||||||
16091|Ridge Hill Sandstone|30939|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16091|Ridge Hill Sandstone|33044|4|Described|p57|||See also map 3||||||
16091|Ridge Hill Sandstone|35638|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16091|Ridge Hill Sandstone|36293|3|Fully described|p208|||||||||
16091|Ridge Hill Sandstone|36890|5|Briefly described|p256|||||||||
16091|Ridge Hill Sandstone|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16091|Ridge Hill Sandstone|37341|6|Mentioned|p236|||||||||
16091|Ridge Hill Sandstone|38997|4|Described|p8|||||||||
16091|Ridge Hill Sandstone|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16091|Ridge Hill Sandstone|44144|4|Described|p501 Tb.4-21, p520 Fig.4-165|Early Pleistocene|Late Cenozoic|Type Section: Ridge Hill 31o55'40''S 116o02'18''E. 10m thick; unfossiliferous. Capped by laterite.||Kwinana Group|||Ferruginous sandstone; thin basal conglomerate.|
16091|Ridge Hill Sandstone|67135|6|Mentioned|p45 Fig.60.|||The subject of a geoheritage site.||||||
16091|Ridge Hill Sandstone|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
16091|Ridge Hill Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||coastal sediment|
16091|Ridge Hill Sandstone|71958|5|Briefly described|p35|Holocene|Holocene|Vlaming Sub-basin. Of the Ridge Hill Shelf.||||||
16103|Ringa Orthogneiss|38513|6|Mentioned|Table II|||||||||
16156|Roadside Bore granite|39162|6|Mentioned|p50|||||||||
16166|Robe Pisolite|14228|6|Mentioned|p9|Eocene|Eocene|||||Grades into Giralia Calcarenite||
16166|Robe Pisolite|22814|6|Mentioned|fig2, p258|||Western Pilbara.||||||
16166|Robe Pisolite|23325|5|Briefly described|map legend|Tertiary|Tertiary|||||||
16166|Robe Pisolite|23529|5|Briefly described|p21|Eocene|Eocene|||||||
16166|Robe Pisolite|23575|5|Briefly described|Map Legend|Cenozoic|Cenozoic|||||||19-NOV-08
16166|Robe Pisolite|23726|5|Briefly described|p8 Fig 2c|Eocene|Eocene|Overlain by Mandu Limestone. Underain by Cardabia Calcarenite. Geological Province: Carnarvon Basin.||||||24-JUL-07
16166|Robe Pisolite|23793|6|Mentioned|p42|Eocene|Eocene|||||||
16166|Robe Pisolite|24025|5|Briefly described|p17|||Geological Province: Pilbara Craton.||||||
16166|Robe Pisolite|24541|6|Mentioned|p62|||Geological Province: Pilbara Craton.||||||
16166|Robe Pisolite|24573|6|Mentioned|p671|Middle Miocene|Late Oligocene|Geological Province: Hamersley Province||||||
16166|Robe Pisolite|29770|6|Mentioned|p77|||||||||
16166|Robe Pisolite|30096|6|Mentioned|p75|||Low prospects for diamonds.||||||
16166|Robe Pisolite|34066|5|Briefly described|Table 1|||Tertiary||||||
16166|Robe Pisolite|34135|5|Briefly described|Table 1|||Tertiary. See also pp19,20.||||||24-JUL-07
16166|Robe Pisolite|35144|6|Mentioned|p5|||||||||
16166|Robe Pisolite|35260|6|Mentioned|p19|||||||||
16166|Robe Pisolite|38776|3|Fully described|p37|||||||||
16166|Robe Pisolite|39426|6|Mentioned|p15|||||||||
16166|Robe Pisolite|39444|6|Mentioned|p46|||||||||
16166|Robe Pisolite|39697|6|Mentioned|p138|||||||||
16166|Robe Pisolite|40355|6|Mentioned|p8|||||||||
16166|Robe Pisolite|40369|6|Mentioned|Plate 2|||||||||
16166|Robe Pisolite|40987|4|Described|p34|||||||||
16166|Robe Pisolite|41271|3|Fully described|p175|||||||||
16166|Robe Pisolite|41438|6|Mentioned|p111|||||||||
16166|Robe Pisolite|42116|5|Briefly described|Fig.1 P6|||||||||
16166|Robe Pisolite|42190|6|Mentioned|p276|||||||||
16166|Robe Pisolite|42260|5|Briefly described|p10|||||||||
16166|Robe Pisolite|42704|5|Briefly described|Plate 2E|Cenozoic|Cenozoic|Pisolitic limonite.||||||19-NOV-08
16166|Robe Pisolite|42898|5|Briefly described|Fig.2 P341|||||||||
16166|Robe Pisolite|43262|5|Briefly described|Map Legend||Cenozoic|||||||19-NOV-08
16166|Robe Pisolite|43290|4|Described|p13|||Age:Late late Eocene?||||||
16166|Robe Pisolite|44438|14|Not recorded|map legend||Tertiary|||||||
16166|Robe Pisolite|44477|4|Described|p.16, Table 1||Cenozoic|SF/50-6.||||||19-NOV-08
16166|Robe Pisolite|44478|14|Not recorded|map legend||Tertiary|||||||
16166|Robe Pisolite|44481|5|Briefly described|map legend||Tertiary|||||||
16166|Robe Pisolite|44501|14|Not recorded|p.7,27, table 4, map||Tertiary|(ref. to de la Hunty 1965). (F/50-7).||||||
16166|Robe Pisolite|44502|14|Not recorded|map legend||Tertiary|||||||
16166|Robe Pisolite|44503|2|Defined|p.8,17,18,Tb.2, map|||Roy Hill Sheet. (F50-12).||||||
16166|Robe Pisolite|44504|14|Not recorded|map legend||Tertiary|||||||
16166|Robe Pisolite|44692|2|Defined|p.7,8,Tb.1, map|||Iron Ore. (F50-11). See also p.20,21,25, for more details.||||||
16166|Robe Pisolite|44729|5|Briefly described|map legend|Tertiary||||||||
16166|Robe Pisolite|61155|5|Briefly described|p3, p8, p16|Late Eocene|Late Eocene|Extensive secondary orebodies. Thickness in Money Shoal Basin: 33m. Geological Province: Pilbara Block/Hamersley Iron Province and Money Shoal Basin - south.||||||
16166|Robe Pisolite|61847|6|Mentioned|p297, p298|||Transported ferruginous regolith of fossil wood fragments. Also known as Channel Iron Deposits.||||||
16166|Robe Pisolite|62021|6|Mentioned|p169|||Channel iron deposits.||||||
16166|Robe Pisolite|62129|6|Mentioned|p23, p24|Late Eocene|Late Eocene|Thickness: 15-45m.||||||07-FEB-11
16166|Robe Pisolite|62130|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Pisolitic limonite deposits developing along river channels.||||||
16166|Robe Pisolite|63236|5|Briefly described|Map legend|Cenozoic|Cenozoic|Channel iron deposits and pisolite.||||||17-SEP-07
16166|Robe Pisolite|63372|5|Briefly described|Map Legend|Late Eocene|Middle Eocene|Pisolitic limonite deposits, developed along palaeodrainage lines; locally clay and shale.||||||
16166|Robe Pisolite|63417|5|Briefly described|Map legend|Neogene|Paleogene|Pisolitic limonite, minor terrigenous siliciclastic material, goethite and hematite deposits; developed along palaeodrainage lines; dissected by present day drainage.||||||
16166|Robe Pisolite|63420|5|Briefly described|Map legend|Neogene|Paleogene|Pisolitic limonite, minor ferruginous siliciclastic material, goethite and hematite deposits; developed along palaeodrainage lines; dissected by present-day drainage.||||||
16166|Robe Pisolite|63432|5|Briefly described|p734|||Name replaced by Robe Formation? A channel iron deposit in the Hamersley Province.||||||07-FEB-11
16166|Robe Pisolite|64654|5|Briefly described|Map Legend|Paleogene|Paleogene|Pisolithic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.||||||17-NOV-08
16166|Robe Pisolite|64657|5|Briefly described|Map Legend|Neogene|Paleogene|Pisolitic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.||||||
16166|Robe Pisolite|64688|5|Briefly described|Map legend|||Channel iron deposits and pisolite.||||||
16166|Robe Pisolite|65008|6|Mentioned|p25|||||||||
16166|Robe Pisolite|65194|5|Briefly described|p15 Fig.2.3, p16 Fig.2.4, p99-100|Neogene|Paleogene|See also Robe Formation p.101, p102 . Fluvial, outcrops extensively. Compositionally diverse and includes massive and pisolitic ironstone with minor layers of clay, ferruginous shale, pebbles, calcrete and  calcareous clay. Mined for iron ore in Robe River area since 1972. A channel-iron deposit.||||Overlies Marra Mamba Iron Formation unconformably. Overlain by Millstream Dolomite unconformably.||07-APR-16
16166|Robe Pisolite|65830|6|Mentioned|p15|||Of the Hamersley Basin.|||||Channel Iron Deposits.|
16166|Robe Pisolite|66108|5|Briefly described|Map legend|Neogene|Paleogene|Pisolitic limonite, goethite, and hematite deposits; developed along palaeodrainage lines; dissected by present-day drainage.||||||
16166|Robe Pisolite|67197|5|Briefly described|p9, p14, p19, p22, p29, p33-34, p36|Cenozoic|Cenozoic|Shown on the legend, but not the map, on p9.|||||Alluvial iron formation.|
16166|Robe Pisolite|67200|5|Briefly described|p8 fig 6, |Eocene|Eocene|||||Overlain by Mandu Limestone|Massive pisolite with oncolites.|
16166|Robe Pisolite|67829|5|Briefly described|p447. |||Hosts channel iron deposits of goethite-rich ore bodies, derived from erosion of a ferruginous pisolitic laterite surface.||||||
16166|Robe Pisolite|68282|5|Briefly described|Map Legend|Miocene|Miocene||||||Pisolitic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.|
16166|Robe Pisolite|68283|5|Briefly described|Map Legend|Neogene|Paleogene|Northern Carnarvon Basin.|||||Pisolitic limonite; minor ferruginous siliciclastic material, goethite, and hematite deposits; developed along palaeodrainage lines; dissected by present-day drainage.|
16166|Robe Pisolite|69012|5|Briefly described|Map Legend|Miocene|Miocene||||||Comprises pisolitic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.|
16166|Robe Pisolite|69013|5|Briefly described|Map Legend|Miocene|Miocene||||||Pisolitic limonite, goethite and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.|30-APR-14
16166|Robe Pisolite|69015|5|Briefly described|Map Legend|Miocene|Miocene||||||Pisolitic limonite, goethite, and hematite deposits developed along paleodrainage lines, dissected by present-day drainage.|05-MAY-14
16166|Robe Pisolite|69167|4|Described|geologyp_lut.csv|Miocene|Miocene||||||Pisolitic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage.|
16166|Robe Pisolite|69182|6|Mentioned|Ch3 p13|||||||Grades laterally into the Giralia Calcarenite.||
16166|Robe Pisolite|69538|5|Briefly described|p516-518, p540|||Channel iron deposits, ~54-58 wt% Fe. Represents ~25% of iron ore mined from Hamersley Province in 2011-2012, increasing annually. Name started when MacLeod (1966) used the term pisolite instead of oolite to avoid confusion with the Phanerozoic marine oolitic or ironstone deposits. Name replaced by Robe Formation (Robe area) and Marillana Formation (Yandi area).|||||Regolith-derived iron-rich fluvial sediments with a high content of small ferruginised wood fragments; ranging from granular mudstones to ooid-dominant ore, with subordinate pebble to boulder conglomerate.|
16166|Robe Pisolite|69590|4|Described|100k_geologyp_lut.csv|Miocene|Miocene|Of Northern Caranrvon Basin, Westralian Superbasin.|23-5.33 Ma (biostrat)||||Pisolitic limonite, goethite, and hematite deposits; developed along paleodrainage lines; dissected by present-day drainage|
16166|Robe Pisolite|70826|6|Mentioned|p7 tbl 4|Miocene|Eocene|Pilbara region.||||||30-APR-20
16166|Robe Pisolite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||pisoliths|
16166|Robe Pisolite|72758|5|Briefly described|p7 Tb.1, p54.|Late Eocene|Late Eocene|Indirect evidence suggests a Late Eocene age. This unit 15-45m thick unit appears along old drainage lines in NE Wyloo mapsheet area.||||Unconformable on Precambrian units.|Includes limonite and hematite pisoliths, generally small amounts of terrigenous detritus, and scattered fragments of fossil wood.|
16166|Robe Pisolite|73574|6|Mentioned|p763, p771 Fig.6|Miocene|Miocene|Host to significant CID mineralisation. See also Robe Formation.||||||
16192|Robinson Range Formation|7161|5|Briefly described|p96, p96 Fig.6|||Approximately 1000m thick (from p96 Fig.6).||||Overlain by the Millidie Creek Formation. Underlain by the Wilthorpe Formation.|Systematically shallows-up from chert pelagite and iron-rich shale, and then to banded iron-formation and iron-rich shale, and then to oolitic, granular and laminated chert, jaspilite and clastic ironstone.|
16192|Robinson Range Formation|12099|5|Briefly described|p678 Fig.4, p682-3, p686|Statherian|Orosirian|||Unit in Padbury Group.||Overlies Wilthorpe Formation. Is overlain by Millidie Creek Formation.|Includes banded iron-formation.|04-MAR-13
16192|Robinson Range Formation|22493|5|Briefly described|p96 Fig.6|||||||||
16192|Robinson Range Formation|22694|5|Briefly described|p7|||||||||
16192|Robinson Range Formation|22940|4|Described|Fig.6 p14, p17|Paleoproterozoic|Paleoproterozoic|See also Table 2 p12. of Padbury Group.||||||07-NOV-08
16192|Robinson Range Formation|23151|5|Briefly described|p67|||of Padbury Group.||||||
16192|Robinson Range Formation|23592|5|Briefly described|p12|||Of Padbury Group. Geological Province: Padbury Basin.||||||
16192|Robinson Range Formation|23744|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
16192|Robinson Range Formation|23747|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||07-NOV-08
16192|Robinson Range Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin||||||
16192|Robinson Range Formation|23749|4|Described|p13|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||
16192|Robinson Range Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Padbury Group. Geological Province: Padbury Basin.||||||
16192|Robinson Range Formation|23890|5|Briefly described|p21 Fig.11|||Of Padbury Group. Geological Province: Padbury Basin.||||||
16192|Robinson Range Formation|29663|2|Defined|p53|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16192|Robinson Range Formation|30010|4|Described|p45|||||||||
16192|Robinson Range Formation|35975|4|Described|p104|||||||||
16192|Robinson Range Formation|36551|6|Mentioned|Table 29|||||||||
16192|Robinson Range Formation|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
16192|Robinson Range Formation|37213|5|Briefly described|p20|||||||||
16192|Robinson Range Formation|37460|4|Described|p144|||||||||
16192|Robinson Range Formation|38978|5|Briefly described|p159|||||||||
16192|Robinson Range Formation|40938|6|Mentioned|p69|||||||||
16192|Robinson Range Formation|40989|4|Described|p27|||||||||
16192|Robinson Range Formation|43238|5|Briefly described|p7|||of Padbury Group.||||||
16192|Robinson Range Formation|43830|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
16192|Robinson Range Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Padbury Basin||||||07-NOV-08
16192|Robinson Range Formation|44927|6|Mentioned|Map Legend|||||||||
16192|Robinson Range Formation|49896|5|Briefly described|p2 Tb. 1|||Of Barnett (1975). Supersedes Robinson Range Beds. Of the Padbury Group.||||||
16192|Robinson Range Formation|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Padbury Group.  Overlies the Wilthorpe Formation.  Geological Province: Padbury Basin.||||||07-NOV-08
16192|Robinson Range Formation|61271|6|Mentioned|p106|||Of the Padbury Group.||||||
16192|Robinson Range Formation|62289|5|Briefly described|plate 1, p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of Padbury Group; ferruginous shale and siltstone; minor banded iron-formation; Geol. Prov: Padbury Basin.||||||
16192|Robinson Range Formation|63866|5|Briefly described|p164|||Western Glengarry Basin.||Padbury Group||||
16192|Robinson Range Formation|64580|4|Described|map legend||Paleoproterozoic|Of Padbury Group. Banded iron-formation; Granular iron-formation; Ferruginous shale and siltstone.||||||09-DEC-08
16192|Robinson Range Formation|65408|5|Briefly described|p83.|Paleoproterozoic|Paleoproterozoic|||Unit in Padbury Group.|||Ferruginous shale, BIF.|
16192|Robinson Range Formation|65411|5|Briefly described|p88, p90, p91, p94.|Paleoproterozoic|Paleoproterozoic|||Unit in Padbury Group.||Conformably overlies Heines and Beatty Park Members (of Wilthorpe Formation). Is conformably overlain by Millidie Creek Formation.|Banded iron-formation, granular iron-formation, shale.|
16192|Robinson Range Formation|65419|4|Described|p37, p42, p45.|Paleoproterozoic|Paleoproterozoic|Of Barnett (1975) and Gee (1979). Unit relationships redefined||Unit in Padbury Group.||Conformably overlies Heines and Beatty Park Members. Is faulted against the Bryah Group.||15-NOV-13
16192|Robinson Range Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Padbury Group. Ferruginous, thinly bedded shale and siltstone; thin and discontinuous chert layers; minor banded and granular iron-formation; metamorphosed.||||||
16192|Robinson Range Formation|66112|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Padbury Group. Ferruginous shale, siltstone, banded iron-formation, and chert.||||||
16192|Robinson Range Formation|67855|5|Briefly described|p206|||||Padbury Group||Overlies Wilthorpe Conglomerate. Contact transitional.|Megnetite, hematite, chert BIF at base. Granular iron formation with lenses of oolitic chert, flaggy beds of red jasper and clastic ironstone in upper part.|
16192|Robinson Range Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Padbury Group|||Banded iron-formation; Granular iron-formation; Ferruginous shale and siltstone; minor banded iron-formation.|
16192|Robinson Range Formation|69003|5|Briefly described|p16|||Padbury Basin.||Padbury Group.||Conformably overlies Wilthorpe Formation. Is overlain conformably by Millidie Creek Formation.|BIF.|
16192|Robinson Range Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|||Padbury Group|||Ferruginous shale, siltstone, banded iron-formation, and chert|
16192|Robinson Range Formation|69596|5|Briefly described|p10-11|||Padbury Basin. Shallow-water (lacustrine or marine platform) deposits.|||||Ironstones.|
16192|Robinson Range Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_geologysub_lut.csv, 100k_interpgeol_lut.csv, West Australian Craton, Padbury Basin|1983-1811 Ma||||Ferruginous Shale, siltstone, banded iron formation and chert.|
16192|Robinson Range Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Padbury Basin, Capricorn Orogen.|ca 19831811 Ma (inferred)|Padbury Group|||Ferruginous shale, siltstone, banded ironformation, and chert.|
16192|Robinson Range Formation|70804|4|Described|p2-p3, p8, p18-p20, p22|Early Proterozoic|Early Proterozoic|This unit is defined by the appearance of ferruginous and hematitic shale followed by two iron formations. See also p24-p28, p45, plate 1.||Padbury Group||Conformably overlies the Wilthorpe Formation. Conformably overlain by the Millidie Creek Formation. Correlated with the Frere Formation.|Ferruginous shale, banded iron-formation, siltstone and shale.|
16192|Robinson Range Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||banded iron formation, shale, chert, iron formation|
16192|Robinson Range 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.|||Ferruginous shale, siltstone, banded iron-formation, and chert|
16192|Robinson Range Formation|71484|4|Described|p121,125,129-130,134,137-139|||Geological province: Padbury Basin. Fe-rich shales ommonly occur in the W and central Padbury Basin; granular and banded iron formations occur to the E. Magnetic imagery indicates possible evidence that the base of the formation is an unconformity or a fault. Possibly age equivalent to Frere Formation, deposited in a large extensional basin, deepening to the W and N.||Unit of Padbury Group.||Overlain by Millidie Creek Formation. Underlain by Wilthorpe Formation or Bertibubba Supersuite.|Ferruginous shale and banded iron formation, siltstone, sandstone, chert, shale.|30-AUG-19
16192|Robinson Range Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Padbury Basin.||Padbury Group|||Ferruginous shale, siltstone, banded iron-formation, and chert.|
16207|Rockingham Sand|12759|5|Briefly described|p43; p28 Tb. 7; p32 Fig 15; P36 Fig 17|?||Defined Passmore (1967, 1970). Type section in Bore R1 (AMG Zone 50, 380100m E, 6526850m N). Max onshore thickness is 110m in the Rockingham area. Occupies an eroded channel incised into top of Wanneroo Member (Leederville Formation). Reassigned in this study from Quaternary to Pliocene, from above to below Ascot and Yoganup Formations. Forms a minor semi-unconfined aquifer.||||below Ascot and Yoganup Formations.|Brown to pale-grey, somewhat silty, slightly feldspathic, medium- to coarse-grained subangular sand.|12-MAY-14
16207|Rockingham Sand|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
16207|Rockingham Sand|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||24-NOV-09
16207|Rockingham Sand|29382|6|Mentioned|Table 10|||||||||
16207|Rockingham Sand|29383|6|Mentioned|Table 3|||||||||
16207|Rockingham Sand|32575|2|Defined|p8|Quaternary|Quaternary|See also p53.||||||17-JAN-08
16207|Rockingham Sand|35093|6|Mentioned|Fig.13|||||||||
16207|Rockingham Sand|35970|6|Mentioned|p77|||See also Table 12.||||||
16207|Rockingham Sand|36293|4|Described|p216|||||||||
16207|Rockingham Sand|39156|4|Described|p22|||||||||
16207|Rockingham Sand|39554|6|Mentioned|Map legend|late Tertiary|late Tertiary|||||||
16207|Rockingham Sand|44144|4|Described|p502 Tb.4-21, p520 Fig.4-165|Pleistocene|Pleistocene|Type Section: Rockingham Bore R1: 32o17'19''S 115o43'36''E. 29-110m of shallow marine sediments.||||Overlies Osborne Formation, Leederville Formation (both unconformably). Overlain by Tamala Limestone.|Yellow-brown, medium- to coarse-grained feldspathic quartz sand.|
16207|Rockingham Sand|63745|6|Mentioned|p64 Fig. 3|||||||||07-FEB-11
16207|Rockingham Sand|68254|6|Mentioned|p1036 Fig.2, p1046 Tb.4|Quaternary|Neogene|||||||
16227|Rocky Bore Granite|23592|5|Briefly described|p8|||||||||
16227|Rocky Bore Granite|38540|6|Mentioned|p385|||||||||
16227|Rocky Bore Granite|44927|5|Briefly described|Map Legend||Archean|2615 +/- 2 Ma||||||07-NOV-08
16227|Rocky Bore Granite|50323|5|Briefly described|Map Legend|Archean|Archean|Porphyritic monzogranite with tabular feldspar phenocrysts, medium-grained.  Age: c.2615Ma.  Geological Province: Yilgarn Craton.||||||07-NOV-08
16227|Rocky Bore Granite|64580|4|Described|map legend|Neoarchean|Neoarchean|Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained.||||||09-DEC-08
16227|Rocky Bore Granite|65896|5|Briefly described|Map legend|Archean|Archean|Yilgarn Craton. Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained. c.2615 Ma.||||||
16227|Rocky Bore Granite|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv|Neoarchean|Neoarchean||||||porphyritic monzogranite with tabular feldspar phenocrysts; medium grained|
16227|Rocky Bore Granite|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Narryer Terrane.|c. 2615 Ma||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained.|06-MAY-14
16227|Rocky Bore Granite|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean||||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained.|
16227|Rocky Bore Granite|69583|5|Briefly described|p130; Plates 2, 3|Archean|Archean|Narryer Terrane, Yilgarn Craton.|c.2620 Ma.||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium-grained; metamorphosed.|
16227|Rocky Bore Granite|70795|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2615 Ma||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained; metamorphosed|
16227|Rocky Bore Granite|70796|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton granite. See also 500k_interpgeop14_lut.csv.|2615 +/ 2 Ma (isotopic)||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained; metamorphosed|
16227|Rocky Bore Granite|70826|6|Mentioned|p9|Neoarchean|Neoarchean|Narryer Terrane.|||||Granite.|13-MAY-20
16227|Rocky Bore Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
16227|Rocky Bore Granite|71269|5|Briefly 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, 1m_geologyp12_lut.csv, 2_5m_interpgeop15_lut.csv.|2615+\-2 Ma (isotopic)||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained; metamorphosed|
16227|Rocky Bore Granite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2615+/-2 Ma||||Porphyritic monzogranite with tabular feldspar phenocrysts; medium grained; metamorphosed.|
16251|Roe Calcarenite|23768|5|Briefly described|p27, p52, p65|Late Pliocene|Late Pliocene|Geological Province: Eucla Basin.  See also p30 Fig. 6 and p62-63.||||||
16251|Roe Calcarenite|24094|5|Briefly described|p273, p277|Late Pleistocene|Early Pleistocene|Thin, sandy limestone. Geological Province: Eucla Basin||||||16-MAR-05
16251|Roe Calcarenite|24347|5|Briefly described|p115 Fig.2|Pliocene|Pliocene|||||||
16251|Roe Calcarenite|31562|4|Described|p14|||Pleistocene||||||
16251|Roe Calcarenite|31903|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|31908|4|Described|Table 1|||Pleistocene||||||
16251|Roe Calcarenite|31909|2|Defined|p9|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|32552|2|Defined|p10|Quaternary|Quaternary|See also P23, 35, 81, 114 etc.||||||
16251|Roe Calcarenite|32648|6|Mentioned|p32|||Pleistocene||||||
16251|Roe Calcarenite|32750|4|Described|p306|||||||||
16251|Roe Calcarenite|34194|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16251|Roe Calcarenite|35097|6|Mentioned|p15|||||||||
16251|Roe Calcarenite|35772|6|Mentioned|Table 1|||||||||
16251|Roe Calcarenite|36386|6|Mentioned|p156|||||||||
16251|Roe Calcarenite|36890|3|Fully described|p416|||||||||
16251|Roe Calcarenite|38553|6|Mentioned|p44|||||||||
16251|Roe Calcarenite|38699|6|Mentioned|p28|||||||||
16251|Roe Calcarenite|38700|6|Mentioned|p38|||||||||
16251|Roe Calcarenite|38774|6|Mentioned|p44|||||||||
16251|Roe Calcarenite|38982|6|Mentioned|p56|||||||||
16251|Roe Calcarenite|39522|6|Mentioned|p86|||||||||
16251|Roe Calcarenite|40992|6|Mentioned|Fig.23|||||||||
16251|Roe Calcarenite|41043|6|Mentioned|p87|||||||||
16251|Roe Calcarenite|41075|6|Mentioned|p32|||||||||
16251|Roe Calcarenite|41831|6|Mentioned|p556|||||||||
16251|Roe Calcarenite|42473|6|Mentioned|p15|||||||||
16251|Roe Calcarenite|43498|6|Mentioned|9||Pleistocene|||||||
16251|Roe Calcarenite|43667|6|Mentioned|Fig.3,p12||Pliocene|||||||
16251|Roe Calcarenite|44145|4|Described|p550 tab 4-27, p557-559|Pleistocene|Pliocene|Eucla Basin. Fossiliferous. Max thickness 8m.||||Disconformable on older rocks.|Weakly cemented, poorly bedded, medium to coarse grained, porous, shelly calcarenite: locally dolomitic.|
16251|Roe Calcarenite|61155|5|Briefly described|p5, p17|Pleistocene|Pliocene|Thin, very shallow-water calcarenites. Age: <2Ma. Geological Province:  Eucla Basin.||||||
16251|Roe Calcarenite|61517|5|Briefly described|p309|Late Pliocene|Pliocene|Bioclastic sandy limestone; richly fossiliferous, notably with mollusc shells. Unconformably overlies Wilson Bluff Limestone. Max. thickness: 7.5m.  Geological Province: Eucla Basin.||||||27-MAY-06
16251|Roe Calcarenite|62069|6|Mentioned|p108|Pliocene|Pliocene|In south Western Australia.||||||
16251|Roe Calcarenite|62369|3|Fully described|p407-4119|Early Pleistocene|Pliocene|Unlithified to friable lime sand, rich in macrofossils. Overlies the Abrakurrie Limestone and, locally, Wilson Bluff Limestone. Age: 2.6-1.8Ma (Sr-isotope). Geological Province: Eucla Basin; lies beneath the Roe Plains in the Great Australian Bight.||||||
16251|Roe Calcarenite|67472|5|Briefly described|180|Pliocene|Pliocene|Bioclastic limestone, Roe Plains. Includes new macrofossil gastropod species Notocypraea goudeyi.||||||11-JUL-13
16251|Roe Calcarenite|67789|5|Briefly described|p34, 41|Pliocene|Pliocene|Nullarbor Plain, Eucla Basin. Deposited during a sea level highstand event.||||Locally overlies Nullarbor Limestone.||
16251|Roe Calcarenite|70397|6|Mentioned|p2-3|Pleistocene|Pliocene|Eucla Basin. Warm-temperate seagrass bed deposits. Presently lies just above sea level, forming the surface of the Roe Plain.||||Underlain by Nullabor Limestone.||
16251|Roe Calcarenite|70771|4|Described|p3, p5, p7-p8, p11-p12, p32, |Pleistocene|Pliocene|Roe Plain, Eucla Basin. This highly fossiliferous unit contains fossilised molluscs (gastropods and bivalves), echinoids, benthic foraminifera and coralline algae. This unit was deposited uniformly on the Roe plain, covering approximately 8000 square kilometers at a thickness of 2-3m. Interpreted as the product of shallow marine, subtidal sedimentation in a seagrass dominated environment.  [The author assigns this unit to the Eucla Group however this term is obsolete]. See also p53-p58, p60-p61.||Eucla Group||Disconformably overlies the Wilson Bluff Limestone and the Abrakurrie Limestone.|Weakly lithified, coarse-grained, poorly-bedded and highly fossiliferous calc-arenite.|
16251|Roe Calcarenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||biocarbonate, limestone, coastal sediment|
16251|Roe Calcarenite|71361|4|Described|p5, p15, p21, p67, p110|Early Pleistocene|Late Pliocene|Eucla Basin. Fossil assemblage includes benthic foraminifera, coralline algae and molluscs. Interpreted to have been deposited in a shallow, warm-temperate grass beds.||||Unconformably overlies the Nullarbor Limestone.|Unlithified fossiliferous Calc-arenite.|
16251|Roe Calcarenite|73084|6|Mentioned|p16|Pleistocene|Pliocene|||||||
16251|Roe Calcarenite|73641|5|Briefly described|p6 Fig.4|Pleistocene|Pliocene|Southern Eucla Basin.||||||
16323|Rosamel Member|40314|4|Described|Table 1|||||||||
16323|Rosamel Member|40367|3|Fully described|p80|Holocene|Holocene|Of Safety Bay Sand. Overlies Burragenup Member; underlies Vittoria Member. Thickness: up to 15m. Littoral sand,beach-ridge/dune unit of uncemented sand and shelly sand; also included is a shoaling sequence of sediments.||||||07-AUG-07
16323|Rosamel Member|69788|6|Mentioned|p1027|Holocene|Holocene|Unconsolidated; mobile sands.||Unit in Safety Bay Sand.||||
16383|Rough Range Formation|45153|6|Mentioned|App.3-50|||||||||
16398|Rowles Lagoon Monzogranite|42705|5|Briefly described|map legend|Archean||Reserved as Rowles Lagoon Granite.||||||07-NOV-08
16398|Rowles Lagoon Monzogranite|42988|5|Briefly described|Map Legend|||||||||
16398|Rowles Lagoon Monzogranite|42989|3|Fully described|p21|||||||||
16398|Rowles Lagoon Monzogranite|43101|3|Fully described|p47|||||||||
16398|Rowles Lagoon Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
16398|Rowles Lagoon Monzogranite|60076|5|Briefly described|p45 App. 1|||[Amro]   Medium- to coarse-grained biotite monzogranite; locally plagioclase-phyric; foliated.||||||
16398|Rowles Lagoon Monzogranite|65204|6|Mentioned|p18 Tbl.3.|Neoarchean||1-6mm grains; sparsely porphyritic.||||||
16398|Rowles Lagoon Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Medium- to coarse-grained biotite monzogranite; local plagioclase phenocrysts; foliated.||||||07-FEB-11
16398|Rowles Lagoon Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained biotite monzogranite; local plagioclase phenocrysts; foliated.|07-AUG-15
16398|Rowles Lagoon Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium- to coarse-grained biotite monzogranite; local plagioclase phenocrysts; foliated.|
16398|Rowles Lagoon Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
16398|Rowles Lagoon 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.|3010-2600 Ma (inferred)||||Medium- to coarse-grained biotite monzogranite; local plagioclase phenocrysts; foliated|
16492|Sabina Sandstone|12758|5|Briefly described|p14, p3 Fig. 3|Early Triassic|Early Triassic|Conformably overlain by Lesueur Sandstone; conformably overlies the Willespie Formation.  Max. thickness: 561m.  Geological Province:  Southern Perth Basin.||||||
16492|Sabina Sandstone|14227|5|Briefly described|p10, Enclos. 2|Early Triassic|Early Triassic|Overlies Willespie Formation (Sue Group). Geol. Prov: Bunbury Trough, southern Perth Basin.||||||07-FEB-11
16492|Sabina Sandstone|22820|5|Briefly described|p15|Early Triassic|Early Triassic|Unconformably overlies Sue Group in places. Referred to as Lower Sabina Sandstone.||||||12-AUG-08
16492|Sabina Sandstone|23816|4|Described|p236|Scythian|Scythian|Geological Province: Perth Basin. Unconformably underlain by Sue Coal Measures. Conformably overlain by Lesueur Sandstone. Max. thickness: 249 m.||||||12-AUG-08
16492|Sabina Sandstone|24160|6|Mentioned|p94|Triassic||Northern Perth Basin.||||||
16492|Sabina Sandstone|24443|5|Briefly described|Fig.31|Early Triassic|Early Triassic|Conformably overlies Willespie Formation of Sue Group. Overlain by Wonnerup Member of Lesueur Sandstone. Geological Province: Perth Basin.||||||
16492|Sabina Sandstone|34841|6|Mentioned|Fig.8|||||||||
16492|Sabina Sandstone|36100|6|Mentioned|Fig.2|||||||||
16492|Sabina Sandstone|36293|2|Defined|p120|Early Triassic|Late Permian|Deposition across the Triassic-Permian boundary.||||||
16492|Sabina Sandstone|36890|3|Fully described|p238|||||||||
16492|Sabina Sandstone|40358|6|Mentioned|p22|||||||||
16492|Sabina Sandstone|40359|5|Briefly described|p22|||||||||
16492|Sabina Sandstone|41474|6|Mentioned|p63|||||||||
16492|Sabina Sandstone|41689|6|Mentioned|Table 1|||||||||
16492|Sabina Sandstone|41728|6|Mentioned|p441|||||||||
16492|Sabina Sandstone|41782|6|Mentioned|Table 2|||||||||
16492|Sabina Sandstone|43031|4|Described|p15,Fig.2|||||||||
16492|Sabina Sandstone|43067|5|Briefly described|Fig.12,p124|||||||||
16492|Sabina Sandstone|43096|5|Briefly described|p3|||see also Fig.2||||||
16492|Sabina Sandstone|43212|6|Mentioned|p5||Triassic|||||||
16492|Sabina Sandstone|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p510|Early Triassic|Late Permian|See also p511 Fig.4-147, p513. Type Section: Whicher Range 1; 3666-3915m. 561m thick fluvial deposits. Apparently a continuous section across the Permian-Triassic boundary.||||Conformably overlies Sue Coal Measures. Overlain conformably by Lesueur Sandstone.|Grey, medium- to coarse-grained sandstone and minor grey shale.|
16492|Sabina Sandstone|50107|5|Briefly described|Map legend|Triassic|Permian|Geological Province: Southern Perth Basin.||||||
16492|Sabina Sandstone|60376|5|Briefly described|p17 Fig. 4.|Early Triassic|Late Permian|Geological Province: Perth Basin. Overlain by Lesueur Sandstone. Underlain by Sue Coal Measures.||||||07-FEB-11
16492|Sabina Sandstone|67925|5|Briefly described|Ch2 p10 fig 4, Ch2 p11, Ch2 p31|Scythian|Scythian|See also  Ch2 p44-p45, Ch3 p8, Ch4 p8 fig 2, Ch4 p30 fig 34, Ch5 p20, Ch5 p23, Ch5 p26, Ch5 p32, Ch5 p39, Ch8 p11.||||Overlies the Willespie Formation and the Sue Group. Overlain by the Lesueur Sandstone, Wonnerup Member.||
16492|Sabina Sandstone|69029|6|Mentioned|p332|Olenekian|Induan|Of Perth Basin.||||Overlain by Kockatea Shale. Underlain by Beekeeper Formation.||
16492|Sabina Sandstone|69081|5|Briefly described|p737 Fig.1|Early Triassic|Early Triassic|Geol. Prov: Perth Basin||||Is overlain by Wonnerup Member (Lesueur Sandstone); overlies Willespie Formation (Sue Group).||23-JUL-15
16492|Sabina Sandstone|69182|6|Mentioned|Ch2 p9, Ch2 p13, Ch2 p20-p29|Lower Triassic|Lower Triassic|Perth Basin. Good reservoir unit, however it lacks a regional sealing unit and as such is not prospective for the storage of carbon dioxide. See also Ch2 p34-p41, Ch2 p44, Ch2 p46, Ch2 p50, Ch2 p54-p55, Ch2 p57, Ch2 p60-p67, Ch2 p74, Ch2 p83-p88, Ch2 p107, Ch2 p109.||||||
16492|Sabina Sandstone|69297|6|Mentioned|p175, p189|Olenekian|Changhsingian|Vlaming Sub-basin, South Perth Basin.||||Overlies the Willespie Formation. Overlain by the Lesueur Sandstone.||
16492|Sabina Sandstone|70097|5|Briefly described|p2, p19 Fig.3|Anisian|Changhsingian|Sandier (compared with Kockatea Shale) facies of marine transgression in southern part of Perth Basin. Mandurah Terrace and Bunbury Trough.||||Overlies Willespie Formation (Sue Group). Is overlain by Lesueur Sandstone.|Sandstone.|12-SEP-17
16492|Sabina Sandstone|70099|5|Briefly described|Fig.4; p5|Olenekian|Changhsingian|Southern Perth Basin. Correlated to seismic package Mentelle 1B, with Willespie Formation and Lesueur Sandstone.||||Overlies Willespie Formation. Is overlain by Lesueur Sandstone.||
16492|Sabina Sandstone|70128|5|Briefly described|p449, p453, p455, p457, p459-463|Early Triassic|Early Triassic|Southern Perth Basin. Modelled thickness distribution histogram.||||Conformably overlies Willespie Formation (Sue Group). Is overlain conformably by Lesueur Sandstone. Time-equivalent of Kockatea Shale.||
16492|Sabina Sandstone|71146|5|Briefly described|p6|Early Triassic|Early Triassic|Perth Basin.||||Overlies the Willespie Formation. Overlain by the Lesueur Sandstone.|Sandstone.|
16492|Sabina Sandstone|71377|4|Described|p1-p3, p7, p77-p82|Early Triassic|Early Triassic|Perth Basin. SHRIMP age is interpreted as the maximum depositional age derived from detrital zircons in this study. SHRIMP age is inconsistent with the biostratigraphic age of Early Triassic. Intersected in GSWA Harvey 1 (2895-2945m). Zircon morphology and sample descriptions are provided. Equivalence with the Kockatea Shale is interpreted on the basis of palynology. See also p86-p88, p90, p102-p103.|537 +/- 9 Ma (SHRIMP U-Pb)|||Conformably overlain by the Wonnerup Member of the Lesueur Sandstone. Conformably overlies the Willespie Formation of the Sue Group. Equivalent to the Kockatea Shale.|Fine- to coarse-grained, moderately-sorted, poorly consolidated sandstone with interbedded siltstone and shale.|
16492|Sabina Sandstone|71958|5|Briefly described|p34|Olenekian|Induan|Vlaming Sub-basin.||||Overlies the Willespie Formation (Sue Group). Overlain by the Lesueur Sandstone.||
16492|Sabina Sandstone|72258|5|Briefly described|p129,133,135,138|Early Triassic|Early Triassic|Of Perth Basin. Demonstrates up-sequence increase in Archean and Ediacaran-Cambrian detritus from the Lower Triassic Sabina Sandstone to Lower Jurassic Eneabba Formation. 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). 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). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen.||||Overlain by Lesueur Sandstone or Woodada Formation. Underlain by Willespie Formation. Laterally grades into Kockatea Shale.||
16492|Sabina Sandstone|73424|6|Mentioned|p5|Early Triassic|Early Triassic|Perth Basin.||||||
16494|Saddle Creek Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|23937|6|Mentioned|p78 App. 1|||Of the Auvergne Group.||||||
16494|Saddle Creek Formation|24122|3|Fully described|p10, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlies Angalarri Siltstone, conformably overlain by Pinkerton Formation.  Maximum thickness 50m.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Parent: Auvergne Group.   Geological Province: Victoria Basin||||||
16494|Saddle Creek Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Angalarri Siltstone;  overlain by Pinkerton Sandstone. Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|28255|5|Briefly described|p67, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Auvergne Group. Consists of oolitic dolomite with minor sandstone and siltstone. Max. thickness: >150m. See also p68 Tb. 6.||||||
16494|Saddle Creek Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
16494|Saddle Creek Formation|32307|4|Described|Table 2|||Proterozoic||||||
16494|Saddle Creek Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
16494|Saddle Creek Formation|32660|5|Briefly described|Table 6|||||||||
16494|Saddle Creek Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Basal crossbedded sandstone; upper siltstone and oolitic dolomite.||||||02-DEC-04
16494|Saddle Creek Formation|32700|4|Described|Table 1|||Previously mapped as Yambarra Beds (Randal, 1962).||||||29-NOV-06
16494|Saddle Creek Formation|32701|4|Described|Table 1|||Adelaidean. Of the Auvergne Group.||||||29-NOV-06
16494|Saddle Creek Formation|32728|6|Mentioned|Fig.14|||||||||
16494|Saddle Creek Formation|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Basal crossbedded sandstone, overlain by siltstone with minor shale and dolomite.||||||02-DEC-04
16494|Saddle Creek Formation|33373|3|Fully described|p10|||p10.||||||29-NOV-06
16494|Saddle Creek Formation|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Auvergne Group. Blocky white quartz sandstone overlain by brown oolitic dolomite. Conformable on Angalarri Siltstone.  Max. thickness: ~50m.||||||26-APR-05
16494|Saddle Creek Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16494|Saddle Creek Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Basal blocky quartz sandstone, brown oolitic dolomite.||||||27-APR-05
16494|Saddle Creek Formation|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16494|Saddle Creek Formation|40494|4|Described|p11|||||||||
16494|Saddle Creek Formation|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Quartz arenite, flaggy to thickly bedded, with large scale cross-bedding, ripple marks and slump structures (up to at least 210m).||||||07-OCT-05
16494|Saddle Creek Formation|41661|5|Briefly described|Table 1|||||||||
16494|Saddle Creek Formation|45112|4|Described|Table 15|||||||||
16494|Saddle Creek Formation|48938|2|Defined|p40|Adelaidean|Adelaidean|||||||
16494|Saddle Creek Formation|48942|3|Fully described|p68|||||||||
16494|Saddle Creek Formation|48943|4|Described|p76|||||||||
16494|Saddle Creek Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Angalarri Siltstone. Overlain by Pinkerton Sandstone. Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite||||||21-JUL-04
16494|Saddle Creek Formation|60682|4|Described|p8, 9 Table 2|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Angalarri Siltstone. Conformably overlain by Pinkerton Formation. Max. thickness: >222m. Basal sandstone, upper siltstone and minor oolitic dolostone and dolarenite. Geological Province: Victoria Basin.||||||11-MAY-05
16494|Saddle Creek Formation|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
16494|Saddle Creek Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Basal sandstone, upper siltstone, minor dolostone and dolarenite||||||
16494|Saddle Creek Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.||
16494|Saddle Creek Formation|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.|Basal quartz sandstone, brown oolitic dolostone, dolomitic sandstone and upper siltstone.|
16494|Saddle Creek Formation|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Basal sandstone, upper siltstone, minor ooidal dolostone and dolarenite.|
16494|Saddle Creek Formation|68733|5|Briefly described|p177 Fig.2, p179, p185, p189 Fig.8, p192|Cryogenian|Cryogenian|Victoria Basin. Sm-Nd isotope data tabulated. Appears as Saddle Creek Sst in Fig.8.||Of the Auvergne Group.||||06-DEC-17
16494|Saddle Creek Formation|69418|6|Mentioned|p3:31|||Victoria Basin. Hosts barite at the Saddle Creek deposit (briefly described).||||||12-JUL-16
16494|Saddle Creek Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone.||12-JUL-16
16494|Saddle Creek Formation|69441|5|Briefly described|p26:2-6|Neoproterozoic|Neoproterozoic|Typically <160m thick; over 222m locally. Very shallow to emergent, high-energy clastic phases with brine-logging, ooid shoals; argillaceous phases are slightly deeper water. Pods and veins of barite occur, but no commercial exploitation has been reported.||Auvergne Group.||Conformably (locally unconformably) overlies Angalarri Siltstone. Is overlain conformably by Pinkerton Sandstone.|Basal sandstone less than 10m thick; overlain by siltstone, oolitic dolostone, silica-cemented quartz sandstone, dolarenite and minor shale. Numerous sedimentary structures.|12-JUL-16
16494|Saddle Creek Formation|69442|5|Briefly described|p27:2-5|||||Auvergne Group.||Is overlain unconformably by Uniya Formation and Skinner Sandstone. Is onlapped unconformably by Beasly Knob Member (Ranford Formation).||12-JUL-16
16494|Saddle Creek Formation|69673|5|Briefly described|p188|||222m thick.||Auvergne Group|||Basal sandstone overlain by siltstone, oolitic dolostone, silica cemented quartz sandstone, dolarenite and minor shale.|
16494|Saddle Creek Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite.|
16494|Saddle Creek Formation|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group||Overlies Angalarri Siltstone. Is overlain by Pinkerton Sandstone, Moonlight Valley Tillite, Kinevans Sandstone, Antrim Plateau Volcanics.|Basal quartz sandstone, brown oolitic dolostone, dolomitic sandstone and upper siltstone.|
16494|Saddle Creek Formation|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Conformably overlies Angalarri Siltstone. Is overlain conformably by Pinkerton Sandstone.|Basal sandstone, upper siltstone, minor oolitic dolostone and dolarenite.|
16494|Saddle Creek Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
16494|Saddle Creek Formation|71302|4|Described|p1,6-7,50-57,72,74|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Typically less than 160m thick, but reaches 222m maximum thickness in AUVERGNE 1:250 000 map sheet (Dunster et al., 2000). probably deposited in very shallow to emergent conditions, with high energy clastic phases and slightly deeper stable conditions (Dunster et al., 2000; Cutovinos et al., 2002). Sample GA 1957133 (quartz sandstone) yielded an interpreted (weighted mean 238U/206Pb) maximum depositional age of 1049+\-20 Ma. Dominated by detritus in the range 1550-1650 Ma, and have very little pre-1800 Ma zircon.||Unit of Auvergne Group.||Overlain by Pinkerton Sandstone. nderlain conformably, to locally unconformably by Angallari Siltstone.|Basal sandstone overlain by siltstone, oolitic dolostone, silica-cemented quartz sandstone, dolarenite and minor shale.|
16494|Saddle Creek Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1053+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
16494|Saddle Creek Formation|73083|6|Mentioned|p7||||||||Siltstone, shale, minor dolostone, sandstone, and dolarenite.|
16497|Saddleback Group|23785|5|Briefly described|p15 Tb. 2|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
16497|Saddleback Group|23989|6|Mentioned|p12|||(Wilde, 1976). Geological Province: Yilgarn Craton||||||
16497|Saddleback Group|33800|2|Defined|p136|Archean|Archean|Sequence of sedimentary, pyroclastic and volcanic (both felsic and mafic) rocks, metamorphosed to greenschist or lower amphibolite facies. The Group is fault bounded.|||Includes Hotham, Wells and Marradong Formations.|||14-FEB-18
16497|Saddleback Group|37017|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16497|Saddleback Group|38497|5|Briefly described|p47|||||||||
16497|Saddleback Group|40359|5|Briefly described|p9|||||||||
16497|Saddleback Group|40360|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
16497|Saddleback Group|40370|4|Described|p7|||||||||
16497|Saddleback Group|40775|4|Described|p494|||||||||
16497|Saddleback Group|40785|6|Mentioned|Fig.6|||||||||
16497|Saddleback Group|41378|5|Briefly described|p77|||||||||
16497|Saddleback Group|43061|5|Briefly described|p12,Table 7|||||||||
16497|Saddleback Group|43189|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
16497|Saddleback Group|43212|6|Mentioned|p3||Archean|Greenstones.||||||07-NOV-08
16497|Saddleback Group|73057|6|Mentioned|p7|Neoarchean|Neoarchean|Yilgarn Craton. Ca. 2675-2650 Ma age is for pyroclastic and intrusive rocks in upper part.|?ca. 2675-2650 Ma||||Granitic intrusions, calc-alkaline magmatism, pyroclastic and intrusive rocks in upper part constrain the minimum age of this Group.|
16508|Safety Bay Sand|12759|5|Briefly described|p51; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Of Passmore (1967, 1970) and Playford and Low (1972). Type section in Rockingham bore R3, (AMG Zone 50, 378077 m E, 6427627 m N,  at 0-24 m). Occurs as eolian stable and mobile dunes.||||Unconformably overlies Tamala Limestone and Becher Sand.|White, unlithified, calcareous fine- to medium-grained quartz sand and shell fragments with traces of fine-grained, black, heavy minerals.|12-MAY-14
16508|Safety Bay Sand|22742|4|Described|p116-119|Holocene|Holocene|~3670 BP. Unconformably overlies Leschenault Formation. 7 unnamed subunits described in the Minninup area.||||||05-NOV-14
16508|Safety Bay 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
16508|Safety Bay Sand|23578|5|Briefly described|p9|Cenozoic|Cenozoic|||||||19-NOV-08
16508|Safety Bay Sand|23816|6|Mentioned|p255|||Geological Province: Perth Basin.||||||
16508|Safety Bay Sand|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
16508|Safety Bay Sand|24410|5|Briefly described|p39|Holocene|Holocene|Of the Kwinana Group. Consists of calcareous sand dunes commonly of shell fragments such as foraminifers and molluscs, variable quartz, and minor feldspar. Overlies Tamal Limestone. Geological Province: Perth Basin.||||||24-NOV-09
16508|Safety Bay Sand|29382|6|Mentioned|Fig.13|||||||||
16508|Safety Bay Sand|29693|6|Mentioned|p41|||||||||
16508|Safety Bay Sand|30217|6|Mentioned|p21|||Sand dune systems||||||
16508|Safety Bay Sand|30939|6|Mentioned|Map legend|Recent|Recent|||||||
16508|Safety Bay Sand|30963|6|Mentioned|Map legend|Recent|Recent|||||||
16508|Safety Bay Sand|31910|4|Described|p24|||Refers Playford & Low (1972)||||||
16508|Safety Bay Sand|32575|2|Defined|p9|Quaternary|Quaternary|See also p10,56.||||||07-AUG-07
16508|Safety Bay Sand|32650|2|Defined|p90|Recent|Recent|||||||
16508|Safety Bay Sand|33044|4|Described|p64|||Shown on map 3||||||
16508|Safety Bay Sand|35638|6|Mentioned|Map legend|Recent|Recent|||||||
16508|Safety Bay Sand|35968|6|Mentioned|p64|||||||||
16508|Safety Bay Sand|36293|3|Fully described|p212|||Passmore (1967, 1970) used the name Safety Bay Sand for the Holocene coastal sand dunes and shallow-marine to littoral sands in the Rockingham-Safety Bay area. Usage of the name was extended by Playford and Low (1972) to include similar sands throughout the Perth Basin. Distribution of the formation coincides with that of the Quindalup Dune System.||||||15-AUG-18
16508|Safety Bay Sand|36890|5|Briefly described|p255|||||||||
16508|Safety Bay Sand|37017|6|Mentioned|Map legend|Recent|Recent|||||||
16508|Safety Bay Sand|37308|5|Briefly described|Fig.3|||||||||
16508|Safety Bay Sand|37480|5|Briefly described|p51|||||||||
16508|Safety Bay Sand|37577|6|Mentioned|p85|||||||||
16508|Safety Bay Sand|38777|4|Described|p30|||||||||
16508|Safety Bay Sand|38997|4|Described|p6|||||||||
16508|Safety Bay Sand|38998|6|Mentioned|p25|||||||||
16508|Safety Bay Sand|39155|6|Mentioned|Table 2|||||||||
16508|Safety Bay Sand|39915|6|Mentioned|Map legend|Holocene|Holocene|||||||
16508|Safety Bay Sand|40085|4|Described|p200|||||||||
16508|Safety Bay Sand|40304|5|Briefly described|p43|||See also P38||||||
16508|Safety Bay Sand|40314|4|Described|p200|||||||||
16508|Safety Bay Sand|40340|6|Mentioned|Table 2|||||||||
16508|Safety Bay Sand|40359|5|Briefly described|p29|||||||||
16508|Safety Bay Sand|40360|6|Mentioned|Map legend|Recent|Recent|||||||
16508|Safety Bay Sand|40367|2|Defined|p79|||Locally interfingers with Leschenault Fm. Proposed by author to subdivide this unit into: Burragenup, Rosamel and Vittoria Members, and Koombana Beach Rock and Binningup Calcrete. Max. thickness: 40m. Detailed lithology presented.||||||07-AUG-07
16508|Safety Bay Sand|40400|4|Described|p109, p111|Holocene|Holocene|Of Passmore (1970). Originally included the Becher Sand unit (seagrass bank suite of sand) which was separated out by Semeniuk and Searl (1983). Geol.Prov: Perth Basin. Beach-beachridge-dune suite of sand readily distinguishable from the seagrass suite..||||||06-AUG-07
16508|Safety Bay Sand|40401|6|Mentioned|p121|||||||||
16508|Safety Bay Sand|40731|5|Briefly described|p34|||||||||
16508|Safety Bay Sand|40902|6|Mentioned|p55|||||||||
16508|Safety Bay Sand|41200|6|Mentioned|p25|Holocene|Holocene|||||||06-AUG-07
16508|Safety Bay Sand|41251|4|Described|p36|||||||||
16508|Safety Bay Sand|41271|6|Mentioned|p16|||||||||
16508|Safety Bay Sand|41342|4|Described|p22|||||||||
16508|Safety Bay Sand|41344|6|Mentioned|p66|||||||||
16508|Safety Bay Sand|41346|6|Mentioned|p38|||||||||
16508|Safety Bay Sand|41502|4|Described|Table 1|||||||||
16508|Safety Bay Sand|41504|6|Mentioned|p71|||||||||
16508|Safety Bay Sand|41634|4|Described|p42|||||||||
16508|Safety Bay Sand|41782|4|Described|p26|||||||||
16508|Safety Bay Sand|41783|4|Described|p48|||||||||
16508|Safety Bay Sand|41986|5|Briefly described|p41|||||||||
16508|Safety Bay Sand|42076|5|Briefly described|p3|||||||||
16508|Safety Bay Sand|42687|6|Mentioned|map legend|||||||||
16508|Safety Bay Sand|42688|6|Mentioned|map legend|||||||||
16508|Safety Bay Sand|43062|4|Described|p27,Table 2.p18|||||||||
16508|Safety Bay Sand|43066|5|Briefly described|Fig.2,p102|||||||||
16508|Safety Bay Sand|43096|5|Briefly described|p6|||||||||
16508|Safety Bay Sand|43231|6|Mentioned|p2|||||||||
16508|Safety Bay Sand|43297|4|Described|p17||Holocene|Validity of unit discussed.||||||
16508|Safety Bay Sand|43304|5|Briefly described|Map Legend||Holocene|||||||
16508|Safety Bay Sand|43306|5|Briefly described|Map Legend||Quaternary|||||||
16508|Safety Bay Sand|43308|5|Briefly described|Map Legend||Quaternary|||||||
16508|Safety Bay Sand|43309|5|Briefly described|Map Legend||Quaternary|||||||
16508|Safety Bay Sand|43347|6|Mentioned|10|||||||||
16508|Safety Bay Sand|43495|6|Mentioned|19,21|||||||||
16508|Safety Bay Sand|43504|6|Mentioned|13||Quaternary|||||||
16508|Safety Bay Sand|44144|4|Described|p501 Tb.4-21, p520 Fig.4-165|Holocene|Holocene|Type Section: Rockingham Bore R3 32o16'53''S 115o42'19''E, 0-24m. Deposition continues to present. Forms Quindalup Dune System.||Kwinana Group||Overlies Tamala Limestone and Cooloongup Sand.|Shell sand with quartz and feldspar.|
16508|Safety Bay Sand|50022|5|Briefly described|p305|Holocene|Holocene|Derived from eroded Tamala Limestone and local benthic assemblages.||||||
16508|Safety Bay Sand|61521|5|Briefly described|p4 Tb.1, p40|Holocene|Holocene|Beach ridges and dunes composed of calcareous sand in Cockburn Sound - gravelly, shelly mixed carbonate quartz sand. Overlies Becher Sand. Max. thickness: 6m. Geological Province: Rottnest Shelf region. See also p39 Tb.7.||||||
16508|Safety Bay Sand|63330|5|Briefly described|p192, p214|Quaternary|Quaternary|Of the Quindalup Dunes. Geological Province: Perth Basin/Swan Coastal Plain.||||||31-JAN-08
16508|Safety Bay Sand|63454|5|Briefly described|p71 Tb. 3|||White, cream, orange, fine and medium sand.||||||
16508|Safety Bay Sand|63745|6|Mentioned|p64 Fig. 3|||See also p60 Fig. 6.||||||07-FEB-11
16508|Safety Bay Sand|67135|5|Briefly described|p60, p61 Fig.82.|||Forms the more obvious dune landforms along the Perth Basin coast; principal source of limesand in the southern Swan Coastal Plain. Used for cement and agricultural lime.|||||Calcium carbonate-rich sands; contains fragments of marine molluscs and variable proportion of quartz.|
16508|Safety Bay Sand|68811|5|Briefly described|p90|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
16508|Safety Bay Sand|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
16508|Safety Bay Sand|69788|4|Described|p1024-1025;1027;p1029 Fig.4;p1034;p1037|Holocene|Holocene|Of Passmore (1970). Type section in Rockingham - Safety Bay area. Constitutes Quindalup Dune System; coastal parabolic dunes and relict cuspate beach-ridge plains and shallow-marine to littoral sands.|||Includes Burragenup, Rosamel and Vittoria Members.||Unconsolidated to weakly consolidated calcareous and quartzose sands.|
16508|Safety Bay Sand|69840|4|Described|p184, 185, 186, 188, p190, p195|Holocene|Holocene|See also p196 Fig.13. Age described as Marine Isotope stage 1. 8150+/-270 years BP to recent.|0.00815 +/- 0.00027 Ma to recent||Burragenup Member and Vittoria Member|Overlies Cooloongup Sand.|Aeolian calcarenites with aragonite and high-Mg calcite.|
16508|Safety Bay Sand|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||coastal sediment|
16508|Safety Bay Sand|73206|6|Mentioned|p856|Holocene|Holocene|Of Semeniuk (1995). Dunes.||||||
16515|Sahul Group|5952|5|Briefly described|p215|Triassic|Triassic|Includes Mount Goodwin, Osprey, Pollard, Challis and Nome Formations. Geological Province: Bonaparte Basin.||||||01-MAR-10
16515|Sahul Group|13194|4|Described|p386 Tb. 4-16, p396 fig 4-60|Rhaetian|Triassic|~2200m thick.||||Overlies Kinmore Group; equivalent to Cape Londonderry Formation and units of Troughton Group.|Interbedded sandstone, limestone, dolomite and shale; minor coal, evaporite and volcanics.|
16515|Sahul Group|13222|6|Mentioned|p229 Fig.2.||||||Includes Benalla, Osprey, Pollard, Challis and Nome Formations.|||
16515|Sahul Group|13224|6|Mentioned|p485 fig 3|Rhaetian|Anisian|||||||
16515|Sahul Group|13354|6|Mentioned|p375 Fig.6.|Triassic|Late Permian|Comprises, in ascending order, Mount Goodwin, Osprey, Pollard, Challis and Nome Formations.||91||||28-OCT-14
16515|Sahul Group|22663|5|Briefly described|W97 -1-7 p3||Triassic|||||||01-MAR-10
16515|Sahul Group|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||29-NOV-06
16515|Sahul Group|23378|4|Described|p180 Fig.2|Late Triassic|Early Permian|In the Vulcan Sub-basin.||||||01-MAR-10
16515|Sahul Group|41532|3|Fully described|p301|||||||||
16515|Sahul Group|41690|5|Briefly described|p3|||||||||
16515|Sahul Group|41716|6|Mentioned|p334|||||||||
16515|Sahul Group|41759|6|Mentioned|p270|||||||||
16515|Sahul Group|42034|4|Described|Fig.4 P11|||||||||
16515|Sahul Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
16515|Sahul Group|42057|6|Mentioned|Fig.3 P70|||||||||
16515|Sahul Group|42066|5|Briefly described|Fig.3 P199|||||||||
16515|Sahul Group|42075|5|Briefly described|Fig.4 P245|||||||||
16515|Sahul Group|42442|3|Fully described|p21|||Occurs in NT and WA.||||||29-NOV-06
16515|Sahul Group|42861|5|Briefly described|p3|||||||||
16515|Sahul Group|43699|6|Mentioned|Fig.6,p10||Middle Triassic|||||||
16515|Sahul Group|43707|5|Briefly described|Fig.3,p4||Triassic|||||||
16515|Sahul Group|49637|5|Briefly described|Fig. 3|Late Triassic|Middle Triassic|Geological Province: Vulcan Sub-basin.||||||07-FEB-11
16515|Sahul Group|60386|6|Mentioned|p300|Late Triassic|Early Triassic|Browse Basin/Bonaparte Basin. Non-marine, deltaic-nearshore-shelf, limestone nearshore-shelf.||||||
16515|Sahul Group|60634|6|Mentioned|p1168 Fig.3. |Triassic|Triassic||||Includes Mount Goodwin, Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||
16515|Sahul Group|61550|6|Mentioned|p495 Fig.2. |Rhaetian|Nammalian||||Includes the Nome, Challis, Pollard and Osprey Formations.|Overlies Mount Goodwin Formation. Is overlain by Plover Formation.||
16515|Sahul Group|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Early Triassic|Includes the Pollard, Benella (possibly misspelt and should be Benalla?), Osprey, Challis and Nome Formations.  Age: 245-~203Ma. Geological Province:  Western Bonaparte Basin.||||||01-MAR-10
16515|Sahul Group|66187|5|Briefly described|p413 Fig.2|Norian|Early Triassic|Mount Ashmore Dome, Bonaparte Basin. Includes the Nome, Challis, Pollard and Osprey Formations.||||||
16515|Sahul Group|68223|6|Mentioned|p179 Fig.4||Permian|||||||
16515|Sahul Group|69297|6|Mentioned|p305, p322|Rhaetian|Anisian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.|||Includes the Osprey Formation, Pollard Formation, Challis Formation and the Nome Formation.|Overlies the Kinmore Group. Overlain by the Troughton Group.||
16515|Sahul Group|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.|||Nome, Osprey, Challis, Benalla, Pollard Formations.|Overlies Mount Goodwin Subgroup (Kinmore Group). Is overlain by Plover Formation (Troughton Group).||12-JUL-16
16515|Sahul Group|70061|5|Briefly described|Regional geology; Figs.6-7. Vulcan:Fig.2|Rhaetian|Anisian||||Benalla, Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||12-JUL-16
16515|Sahul Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Rhaetian|Carnian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Osprey, Pollard, Challis and Nome Formations.|Overlies Kinmore Group. Is overlain by Troughton Group.||12-JUL-16
16515|Sahul Group|71146|5|Briefly described|p6|Middle Triassic|Middle Triassic|Bonaparte Basin.||||Overlies the Osprey Formation.|Sandstone.|
16532|Saint George Member|41839|6|Mentioned|p27|||Supersedes Saint Georges Formation""||||||
16537|Saint Ives Group|38453|6|Mentioned|Fig.9|||Refers to a group of nickel deposits;not a stratigraphic name.||||||
16537|Saint Ives Group|42817|6|Mentioned|Table 3|||actually spelt St Ives Group||||||
16537|Saint Ives Group|65834|6|Mentioned|p26|||Kalgoorlie Terrane.||||||
16559|Salgash Subgroup|22615|6|Mentioned|p 7|||||||||
16559|Salgash Subgroup|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3520-3400Ma||||||07-NOV-08
16559|Salgash Subgroup|22717|6|Mentioned|Fig3 P18||Archean|||||||07-NOV-08
16559|Salgash Subgroup|23046|5|Briefly described|169|||||||||
16559|Salgash Subgroup|23255|5|Briefly described|p46 Fig.2|||Of the Warrawoona Group.||||||24-JUL-07
16559|Salgash Subgroup|23388|6|Mentioned|p14 Table 1|||||||||
16559|Salgash Subgroup|23416|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group, Pilbara Craton||||||07-NOV-08
16559|Salgash Subgroup|23755|5|Briefly described|p17 Table 1|Archean|Archean|Age: c.3458 Ma. Of Warrawoona Group.||||||07-NOV-08
16559|Salgash Subgroup|23783|5|Briefly described|p7 Fig. 2|||Of Warrawoona Group.||||||
16559|Salgash Subgroup|23784|5|Briefly described|p70|Archean|Archean|||||||07-NOV-08
16559|Salgash Subgroup|23807|5|Briefly described|p110|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|23813|5|Briefly described|p103|Archean|Archean|||||||07-NOV-08
16559|Salgash Subgroup|23895|5|Briefly described|p885 Fig.2, p904|||Overlies Talga Talga Subgroup.  Geological Province: Pilbara Craton.||||||07-MAR-05
16559|Salgash Subgroup|23936|6|Mentioned|p16|||Geological Province: Pilbara Craton.||||||
16559|Salgash Subgroup|24025|4|Described|p9 Tb.1|||Contains the Euro Basalt, Strelley Pool Chert, Panorama Formation and Apex Basalt. Of the Warrawoona Group.||||||22-OCT-08
16559|Salgash Subgroup|24182|4|Described|p92|||Of the Warrawoona Group. Age: 3490 Ma.  Tholeiitic basalt and komatiite successions. Geological Province: Pilbara Craton.||||||
16559|Salgash Subgroup|24184|4|Described|p699, p707 Fig.8|Archean|Archean|Of the Warrawoona Group. Underlain by Talga Talga Subgroup. Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|24185|5|Briefly described|p744 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|24532|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|24590|5|Briefly described|p129, p30 Fig. 1.3|Archean|Archean|Upper part of Warrawoona Gp. Includes Towers Fm, Apex Basalt, Panorama Fm, Strelley Pool Chert + Euro Basalt. Concordantly overlies Duffer Fm; unconformably underlies Wyman Fm + Sulphur Springs Gp.  Age: 3.46-3.31Ga. Thick: 4-5km.||||||07-FEB-11
16559|Salgash Subgroup|31309|6|Mentioned|Table 8|||||||||
16559|Salgash Subgroup|31853|2|Defined|p60|Archean|Archean|||||||07-NOV-08
16559|Salgash Subgroup|35142|6|Mentioned|Fig.1|||||||||
16559|Salgash Subgroup|35531|6|Mentioned|Fig.1|||Composite lithostratigraphic section||||||
16559|Salgash Subgroup|35681|6|Mentioned|Table 3|||See also P10.||||||
16559|Salgash Subgroup|35726|6|Mentioned|p60|||||||||
16559|Salgash Subgroup|37373|4|Described|p79|||||||||
16559|Salgash Subgroup|37899|6|Mentioned|Fig.2|||||||||
16559|Salgash Subgroup|38242|6|Mentioned|p199|||||||||
16559|Salgash Subgroup|38498|5|Briefly described|Table 1|||||||||
16559|Salgash Subgroup|38510|6|Mentioned|p188|||||||||
16559|Salgash Subgroup|38542|6|Mentioned|p361|||||||||
16559|Salgash Subgroup|38544|6|Mentioned|p295|||||||||
16559|Salgash Subgroup|38624|6|Mentioned|Fig.2|||||||||
16559|Salgash Subgroup|39426|6|Mentioned|Fig.3|||||||||
16559|Salgash Subgroup|39444|6|Mentioned|Table 1|||||||||
16559|Salgash Subgroup|39580|4|Described|p288|||||||||
16559|Salgash Subgroup|39672|6|Mentioned|p238|||||||||
16559|Salgash Subgroup|39697|6|Mentioned|p53|||||||||
16559|Salgash Subgroup|40596|6|Mentioned|p65|||||||||
16559|Salgash Subgroup|41028|5|Briefly described|p227|||||||||
16559|Salgash Subgroup|41252|6|Mentioned|Table 1|||||||||
16559|Salgash Subgroup|41350|6|Mentioned|Fig.4|||||||||
16559|Salgash Subgroup|41624|6|Mentioned|p43|||||||||
16559|Salgash Subgroup|43595|6|Mentioned|Table 2-28,p214|||||||||
16559|Salgash Subgroup|43644|6|Mentioned|p594|||||||||
16559|Salgash Subgroup|43698|6|Mentioned|p3|||||||||
16559|Salgash Subgroup|43769|6|Mentioned|Fig.3,p858|||||||||
16559|Salgash Subgroup|44150|5|Briefly described|p129 Tb.2-15, p137-138|||Defined by Lipple (1975). Consists of 40% ultramafic rocks.||Warrawoona Group|Towers, Panorama Formations; Apex, Euro Basalts.|is overlain by Wyman Formation.||
16559|Salgash Subgroup|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Warrawoona Group.  Includes the Euro Basalt, Panorama Formation and the Apex Basalt.||||||07-NOV-08
16559|Salgash Subgroup|46319|5|Briefly described|p4|Archean|Archean|Of Warrawoona Group.  Age: 3341+/-2Ma, 3276+/-7Ma (Pb/Pb).  Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|50189|5|Briefly described|p7, p8 Fig. 4|Archean|Archean|Of the Warrawoona Group. See also p8 Fig. 4.||||||07-NOV-08
16559|Salgash Subgroup|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Warrawoona Group.  Underlies Euro Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|50379|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|50381|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|50423|5|Briefly described|p216||Archean|>3430 Ma. Of lower Warrawoona Group||||||07-NOV-08
16559|Salgash Subgroup|50427|5|Briefly described|p182 Fig.5|Archean|Archean|Age: 3460-3430 Ma. Overlies Talga Talga Subgroup, overlain conformably and unconformably by Kelley Subgroup. Of Warrawoona Group.||||||07-NOV-08
16559|Salgash Subgroup|50544|5|Briefly described|p9|Archean|Archean|Of the Warrawoona Group.  Included Euro Basalt which it is now proposed should transferred to the new Kelly Subgroup.||||||07-NOV-08
16559|Salgash Subgroup|50555|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group.  Includes the Panorama Formation and Apex Basalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|60112|6|Mentioned|p107 Fig.1 |||||||||
16559|Salgash Subgroup|60429|5|Briefly described|p7|Archean|Archean|See also p8 Fig. 4.||||||07-FEB-11
16559|Salgash Subgroup|61253|5|Briefly described|p51,  p52 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Warrawoona Group. Includes the Towers Formation, Apex Basalt, Panorama Formation and Strelley Pool Chert. Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|63417|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup).  Includes Apex Basalt and Panorama Formation. Age: ~3433-3427Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|63420|5|Briefly described|Map legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup).  Includes the Apex Basalt and Panorama Formation. Age: c.3458 -3427Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
16559|Salgash Subgroup|63441|4|Described|p4 Tb. 1, p20|Archean|Archean|Of Warrawoona Gp. Originally included Towers Fm, Apex Basalt, Panoram Fm.+ Euro Basalt (Hickman 1983). Now redefined as only Apex Basalt and Panorama Formation. Age:3434 to 3427Ma.Conformable on Coongan Subgroup; overlain by Kelly Group. Max.thick: ~4000m||||||07-FEB-11
16559|Salgash Subgroup|63538|4|Described|p5, p6 Fig. 3|Archean|Archean|Of Warrawoona Group. Includes Panorama Formation and Apex Basalt. Underlain by Coongan Subgroup. Age: 3458-3426 Ma. Geological Province: Pilbara Craton. Mafic and felsic volcanic rocks.||||||19-APR-13
16559|Salgash Subgroup|64328|4|Described|p54-55|||Of the Warrawoona Group. Formerly contained Towers Fm, Apex Basalt, Panorama Fm and Euro Basalt; now comprises Apex  Basalt, Panorama Fm and Strelley Pool Chert. Conformably overlain by Kelly Subgroup.||||||18-DEC-12
16559|Salgash Subgroup|64405|5|Briefly described|p2 Fig. 1, p21|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological province: East Pilbara Terrane.||||||07-FEB-11
16559|Salgash Subgroup|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
16559|Salgash Subgroup|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Warrawoona Group. Includes Panorama Formation and Strelley Pool Chert. Geological Province: Pilbara Craton.||||||07-FEB-11
16559|Salgash Subgroup|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Panorama Formation. Geological Province: Pilbara Craton.||||||
16559|Salgash Subgroup|64936|5|Briefly described|map legend|Archean|Archean|Of Warrawoona Group. Includes Panorama Formation and Apex Basalt. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
16559|Salgash Subgroup|65008|5|Briefly described|p2, p7, p8, p41|||East Pilbara Granite-Greenstone Terrane.||Of the Warrawoona Group|Includes the Panorama Formation.|||
16559|Salgash Subgroup|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Warrawoona Group.|Includes Strelley Pool Chert, Panorama Formation and Apex Basalt.|||
16559|Salgash Subgroup|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of Warrawoona Group.|Includes Panorama Formation and Apex Basalt.|||
16559|Salgash Subgroup|65827|4|Described|p6 Tb.1|Paleoarchean|Paleoarchean|Of redefined (Van Kranendonk et al. 2006) Warrawoona Group. Includes Apex Basalt and Panorama Formation. Formerly included Strelley Pool Chert. 3474-3430 Ma. Overlies Coongan Subgroup.||||||21-JAN-22
16559|Salgash Subgroup|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit of Warrawoona Group. Comprises Apex Basalt and Panorama Formation. Roughly coeval with Tambina Supersuite.||||||
16559|Salgash Subgroup|66217|4|Described|p5, p6 Table 1, p8, p14, pp24-27. |Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Van Kranendonk et al. (2002) included the Apex Basalt, Panorama Formation and Strelley Pool Formation in this unit in their redefinition of the Warrawoona Group, but later excluded the Strelley Pool Formation (Van Kranendonk et al. 2006a). Thickness to 3750 m in the type area, due west of Marble Bar, in the Marble Bar greenstone belt.|3458-3426 Ma (Van Kranendonk et al. 2006a).|Unit in Warrawoona Group.|Includes Apex Basalt and Panorama Formation.|Overlies Coongan Subgroup paraconformably. Is overlain unconformably by Strelley Pool Formation.||
16559|Salgash Subgroup|66664|6|Mentioned|p3.  |||East Pilbara Terrane||Unit in Warrawoona Group.||Overlies Coongan Subgroup.||
16559|Salgash Subgroup|66745|5|Briefly described|p54 Fig.4.|Paleoarchean|Paleoarchean|||Unit in Warrawoona Group.|Includes Apex Basalt and Panorama Formation.|Disconformably overlies Coongan Subgroup.||
16559|Salgash Subgroup|67197|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Apex Basalt, Panorama Formation.|||
16559|Salgash Subgroup|67201|4|Described|p7 Fig.4, p13 Fig.8|||In northern Pilbara Craton, East Pilbara Terrane.||Warrawoona Group|Panorama Formation, Apex Basalt|||
16559|Salgash Subgroup|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Warrawoona Group.|Apex Basalt; Panorama Formation.|Overlies Coongan Subgroup. Is overlain by Strelley Pool Formation.||
16559|Salgash Subgroup|67270|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Apex Basalt, Panorama Formation.|Overlies Coongan Subgroup. Is overlain by Strelley Pool Formation.||
16559|Salgash Subgroup|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane.|min age 3427 Ma|Of Warrawoona Group. |Includes Apex Basalt, Panorama Formation.|Disconformably overlies Coongan Subgroup, unconformably overlain by Strelley Pool Formation.|Basalt, felsic volcanics, lesser komatiite, komtiitic basalt,minor jaspilite and siliciclastic rocks.|
16559|Salgash Subgroup|68280|6|Mentioned|p4||||||Includes Apex Basalt, Panorama Formation|||
16559|Salgash Subgroup|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes Panorama Formation, Apex Basalt.|||23-SEP-13
16559|Salgash Subgroup|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group|Includes Panorama Formation, Apex Basalt.|||12-JUN-14
16559|Salgash Subgroup|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes Apex Basalt, Panorama Formation.|||23-SEP-13
16559|Salgash Subgroup|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group.|Panorama Formation, Apex Basalt.|Overlies Coongan Subgroup. Is overlain by Strelley Pool Formation.||
16559|Salgash Subgroup|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean||3449-3427 Ma|Of the Warrawoona Group.|Includes the Panorama Formation and the Apex Basalt.|||28-APR-14
16559|Salgash Subgroup|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes the Panorama Formation, and the Apex Basalt.|||
16559|Salgash Subgroup|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|Includes Panorama Formation, Apex Basalt|||
16559|Salgash Subgroup|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of Warrawoona Group.|Includes Panorama Formation.|||
16559|Salgash Subgroup|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||Warrawoona Group|Panorama Formation, Apex Basalt|||
16559|Salgash Subgroup|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, 250k_interpgeol_lut.csv.||Unit of Warrawoona Group.|Includes Apex Basalt.|||
16559|Salgash Subgroup|70022|6|Mentioned|p115|||East Pilbara Terrane.||Warrawoona Group.|Apex Basalt, Panorama Formation.|||
16559|Salgash Subgroup|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.||||
16559|Salgash Subgroup|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Warrawoona Group.||||
16559|Salgash Subgroup|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Includes Parorama Formation and Apex Basalt.|Overlain unconformably by Strelley Pool Formation. Underlain unconformably by Coongan Subgroup/Marble Bar Chert Member.||
16559|Salgash Subgroup|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||shale, volcaniclastic rock, chert, banded iron formation|
16559|Salgash Subgroup|71487|5|Briefly described|p128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.||Uppermost unit of Warrawoona Group.Overlain unconformably by Strelley Pool Formation. Underlain by Coongan Subgroup.||
16559|Salgash Subgroup|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Panorama Formation, Apex Basalt.|||
16559|Salgash Subgroup|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.|Includes Panorama Formation and Apex Basalt.|Uppermost unit of Warrawoona Group. Overlain unconformably by Strelley Pool Formation. Underlain by Coongan Subgroup.||
16559|Salgash Subgroup|72668|6|Mentioned|p4|||East Pilbara Terrane.||Warrawoona Group|Includes the Apex Basalt and the Panorama Formation.|Overlies the Coongan Subgroup.||
16559|Salgash Subgroup|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|Apex Basalt, Panorama Formation.|Overlies Coongan Subgroup. Is overlain unconformably by Strelley Pool Formation.||
16567|Sally Downs Tonalite|22754|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1821 Ma.||||||07-NOV-08
16567|Sally Downs Tonalite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1821 +/- 4 Ma.||||||07-FEB-07
16567|Sally Downs Tonalite|23751|4|Described|p17|Orosirian|Orosirian|Age: 1821+/-4 Ma (SHRIMP U-Pb). Of Mabel Downs suite.||||||
16567|Sally Downs Tonalite|23925|6|Mentioned|p221 Table 1|Orosirian|Orosirian|Age: 1821 +/- 4 Ma.  Geological Province: Halls Creek Orogen.||||||
16567|Sally 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
16567|Sally Downs Tonalite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.||||||07-NOV-08
16567|Sally Downs Tonalite|41977|5|Briefly described|p473|||||||||
16567|Sally Downs Tonalite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
16567|Sally Downs Tonalite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
16567|Sally Downs Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
16567|Sally 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).||||||11-JUN-14
16567|Sally Downs Tonalite|63866|5|Briefly described|p132|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1821 Ma|Sally Downs Supersuite||||
16567|Sally Downs Tonalite|66845|4|Described|p537 Fig.3, p539 Tb.1, p541 Fig.6, p542|||Detailed SHRIMP analysis data. Individual results for grains no. 55 and 56 of 1819+/-8 and 1819+/-10 Ma, 207Pb/206Pb.|Magmatic crystallis'n age, 1821+/-4 Ma SHRIMP U-Pb||||Hornblende-biotite tonalite.|04-AUG-15
16567|Sally Downs Tonalite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547).|~1821 Ma|Of Mabel Downs suite.||||
16567|Sally Downs Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data migrated from OZCHRON1. Original comment: 'All 22 data points are concordant, and define a single population in 207/206 that determines this to be the igneous crystallisation age of the granodiorite or tonalite. No zircon inheritance is observed in this rock.'|Crystallisation age 1821+/-4 Ma U/Pb SHRIMP|Mabel Downs Suite|||Medium-grained, equigranular biotite-hornblende tonalite; minor biotite-bearing quartz diorite and leucocratic biotite granite.|04-AUG-15
16567|Sally Downs Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1821 Ma|Mabel Downs Suite|||Medium grained, equigranular biotite-hornblende tonalite; minor biotite bearing quartz diorite and leucocratic biotite granite.|
16567|Sally 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.|1821-1821 Ma (Isotopic)|Unit of Mabel Downs Suite.|||Medium-grained, equigranular biotite-hornblende tonalite; minor biotite-bearing quartz diorite and leucocratic biotite granite|
16567|Sally Downs Tonalite|69932|6|Mentioned|p312|||Halls Creek area, East Kimberley. Has geochemical similarities with some high Sr/low Y Arunta Inlier granites.|1860 Ma.|||||
16567|Sally Downs Tonalite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1821 Ma|Mabel Downs Suite|||Medium grained, equigranular biotite, hornblende tonalite; minor biotite bearing quartz diorite and leucocratic biotite granite.|
16567|Sally 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.|1821+\-4 Ma to 1821+\-4 Ma (isotopic)|Unit of Mabel Downs Suite.|||Medium-grained, equigranular biotite-hornblende tonalite; minor biotite-bearing quartz diorite and leucocratic biotite granite|
16567|Sally Downs Tonalite|71397|6|Mentioned|p8|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen.||||||
16567|Sally Downs Tonalite|72437|5|Briefly described|p10, p97-98|Palaeoproterozoic|Palaeoproterozoic||c. 1835-1815 Ma|Mabel Downs suite|||Biotite-hornblende tonalite.|
16579|Samuel Formation|7433|5|Briefly described|p25 Fig.2, p42, p47.|Aptian|Aptian|Canning Basin and, more extensively, Officer Basin. Marine fine clastics. Contains pelecypods, gastropods and palynomorphs.||||Laterally equivalent to Anketell Sandstone. Underlies Bejah Claystone.|Thin-bedded, shallow-marine, fine sandstone and mudstone.|
16579|Samuel Formation|22707|6|Mentioned|P16|||||||||
16579|Samuel Formation|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
16579|Samuel Formation|22801|6|Mentioned|P13||Early Cretaceous|Equivalent to the Anketell Sandstone||||||
16579|Samuel Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
16579|Samuel Formation|24067|5|Briefly described|p252|Aptian|Aptian|Geological Province: Officer Basin.||||||
16579|Samuel Formation|24161|5|Briefly described|p28|Early Cretaceous|Early Cretaceous|Unconformably overlies the Paterson Formation.||||||
16579|Samuel Formation|31153|6|Mentioned|p111|||Refers bivalves of Offices Basin||||||
16579|Samuel Formation|31455|4|Described|Table 2|||||||||
16579|Samuel Formation|31456|4|Described|Table 1|||||||||
16579|Samuel Formation|31459|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16579|Samuel Formation|31632|4|Described|Table 2|||See also p12.||||||09-FEB-18
16579|Samuel Formation|31633|4|Described|Table 2|||||||||
16579|Samuel Formation|31635|4|Described|Table 2|||||||||
16579|Samuel Formation|31636|5|Briefly described|p7|||See also Table 2||||||
16579|Samuel Formation|31638|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31639|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31642|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|31914|2|Defined|p98|Aptian|Aptian|||||||
16579|Samuel Formation|33587|3|Fully described|p9|||Table 2.||||||
16579|Samuel Formation|33588|4|Described|p9|||Table 2.||||||
16579|Samuel Formation|33595|6|Mentioned|p16|||||||||
16579|Samuel Formation|33596|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|33597|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35127|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35222|4|Described|Table.2|||||||||
16579|Samuel Formation|35223|6|Mentioned|Table.2|||||||||
16579|Samuel Formation|35250|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35387|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16579|Samuel Formation|35497|6|Mentioned|Table 1|||||||||
16579|Samuel Formation|35902|4|Described|Table 1|||||||||
16579|Samuel Formation|35903|4|Described|Table 1|||||||||
16579|Samuel Formation|36257|6|Mentioned|Table 2.1|||||||||
16579|Samuel Formation|36701|6|Mentioned|Map legend|Early Cretaceous|Early Permian|Early Cretaceous to Early Permian||||||
16579|Samuel Formation|36890|3|Fully described|p353|||See also p406.||||||10-FEB-20
16579|Samuel Formation|37916|5|Briefly described|Fig.2|||||||||
16579|Samuel Formation|38878|6|Mentioned|Map legend|Albian|Aptian|Albian - Aptian||||||
16579|Samuel Formation|38898|6|Mentioned|Table 1|||||||||
16579|Samuel Formation|39211|5|Briefly described|p53|||||||||
16579|Samuel Formation|42194|6|Mentioned|p8|||||||||
16579|Samuel Formation|42431|5|Briefly described|p237|||||||||
16579|Samuel Formation|42734|5|Briefly described|map legend|Cretaceous||||||||
16579|Samuel Formation|43563|6|Mentioned|Fig2,p5||Early Cretaceous|||||||
16579|Samuel Formation|43656|6|Mentioned|Fig.2,p8|Aptian|Barremian|||||||
16579|Samuel Formation|43746|6|Mentioned|Fig.2,p11|Aptian|Barremian|||||||
16579|Samuel Formation|44145|6|Mentioned|p553|||Officer Basin rocks. Must be Early Cretaceous (age of Madura Formation)||||To south, grade laterally into Madura Formation.||
16579|Samuel Formation|44354|5|Briefly described|Map Legend||Early Cretaceous|||||||
16579|Samuel Formation|45104|5|Briefly described|p30|||||||||
16579|Samuel Formation|45149|2|Defined|p53|Early Cretaceous|Early Cretaceous|See also table 1 and P9.||||||
16579|Samuel Formation|45153|2|Defined|App.8-140|Aptian|Aptian|||||||
16579|Samuel Formation|45158|3|Fully described|p12|||||||||
16579|Samuel Formation|45168|6|Mentioned|p6, Table 1|||||||||
16579|Samuel Formation|46975|6|Mentioned|p86|||||||||
16579|Samuel Formation|64580|4|Described|map legend||Early Cretaceous|Siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic.||||||09-DEC-08
16579|Samuel Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
16579|Samuel Formation|64970|6|Mentioned|p719 Fig. 2|Cretaceous|Jurassic|Geological Province: Officer Basin.||||||27-MAY-09
16579|Samuel Formation|65102|4|Described|p366,369,374, Figure 4-41, p369|Aptian|Valanginian|Officer Basin. 2-80m; variegated siltstone, sandstone & claystone; micaceous, carbonaceous & glauconitic beds; marine, shallow water; disconformable on Paterson Formation; type section at Mount Charles, 25deg 46min S, 125deg 06min E.||||||
16579|Samuel Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
16579|Samuel Formation|65416|5|Briefly described|p144.|Cretaceous|Cretaceous|Central and northwest Officer Basin.|||||Thin unit of interbedded marine sandstones and claystones.|
16579|Samuel Formation|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Callawa and Cronin Formations. Is overlain by Bejah Claystone.||
16579|Samuel Formation|67195|4|Described|p19 table 1, p45, 46, 47|||Western Officer Basin. Thermal conductivity of 1.28 W/mK. See also App 1, App 2.|||||Grey to yellow laminated claystone, siltstone and fine grained sandstone; sulphurous, occasional bioturbation, micaceous glauconite?; reddish brown to ochre siltstone, claystone with finely laminated interbeds of whispy fine-grained sandstone.|
16579|Samuel Formation|67200|5|Briefly described|app 2 p10||||||||Laminated claystone, siltstone and fine grained sandstone; sulphorous and occasionally bioturbated.|
16579|Samuel Formation|68007|6|Mentioned|p4, p8|Early Cretaceous|Early Cretaceous|Canning Basin. Barremian to Aptian.||||(Most probably) overlies Callawa Formation.||19-FEB-20
16579|Samuel Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Callawa and Cronin Formations; is overlain by Bejah Claystone.||
16579|Samuel Formation|69029|6|Mentioned|p319|Aptian|Barremian|Of Canning Basin.||||Overlain by Baja Claystone. Underlain by Broome Sandstone.||
16579|Samuel Formation|69091|6|Mentioned|p106 Fig.5.7a, see comments|||See also p107 Fig.5.8a, p109 Fig.5.10.||||||
16579|Samuel Formation|69153|6|Mentioned|500k_geologyp08_lut.csv||Early Cretaceous|Lithology description shared with Bejah Claystone|||||Siltstone, sandstone and claystone; micaceous, carbonaceous|
16579|Samuel Formation|69182|6|Mentioned|Ch4 p9, Ch4 p45, Ch4 p47|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Callawa and Cronin Formations. Overlain by the Bejah Claystone.||10-FEB-20
16579|Samuel Formation|69312|5|Briefly described|p3|Aptian|Barremian|Canning Basin.||||Overlies the Broome and Barbwire Sandstones. Overlain by the Baja Claystone.|Shale and sandstone.|
16579|Samuel Formation|70634|4|Described|500k_geolgyp08_lut.csv|Early Cretaceous|Early Cretaceous|Included with Bejah Claystone in file (undivided)|||||undivided; siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic, radiolarian siltstone in Bejah Claystone|09-FEB-18
16579|Samuel Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Callawa and Cronin Formations. Overlain by the Bejah Claystone.||10-FEB-20
16579|Samuel Formation|70793|4|Described|500k_interpgeop14_lut.csv|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)||||Siltstone, sandstone and claystone; carbonaceous, locally glauconitic; radiolarian siltstone in Bejah Claystone|
16579|Samuel Formation|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Gunbarrel Basin.||||||
16579|Samuel Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, claystone, siltstone|
16579|Samuel Formation|71268|4|Described|GEOL_LUT_CSV files|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)|||Correlable with Bejah Claystone.|Siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic.|
16579|Samuel Formation|72034|6|Mentioned|500k_interpgeop16_lut|Albian|Aptian|Gunbarrel Basin. Shown as informal combination with Bejah Claystone.  Age from biostratigraphy.||||||
16579|Samuel Formation|72497|5|Briefly described|p3 Fig.2.|Aptian|Barremian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins.||||Conformably overlies Cronin and Callawa Formation and underlies Bejah Claystone. Laterally equivalent to Melligo-Para-Frozier Sandstone.||
16579|Samuel Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Willara Sub-basin and the Broome Platform.||||Overlies Callawa and Cronin Formations and partially overlies Broome Sandstone. Laterally equivalent to Frezier Sandstone.|Includes shale.|
16579|Samuel Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Callawa/Cronin formations. Overlain by Bejah Claystone. Equivalent to Frezier Sandstone, Parda Formation, and Melligo Sandstone.|Dominantly shale and mudstone.|
16579|Samuel Formation|73346|6|Mentioned|p28|Cretaceous|Cretaceous|Ryan Shelf.||||Unconformably underlain by Grant Group.||
16648|Sawpit Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
16648|Sawpit Member|43162|6|Mentioned|6|||||||||
16679|Scorpion Group|22478|6|Mentioned|p23||Mesoproterozoic|||||||
16679|Scorpion Group|22491|5|Briefly described|p 9||Mesoproterozoic|Yilgarn Craton||||||
16679|Scorpion Group|22896|6|Mentioned|103|||Geol province Bangemall Basin||||||
16679|Scorpion Group|23529|5|Briefly described|p7|||Parent: Bangemall Supergroup.  Geological Province: Bangemall Basin||||||11-APR-08
16679|Scorpion Group|24017|5|Briefly described|p3 Fig. 1|||Of the Bangermall Supergroup.||||||07-AUG-08
16679|Scorpion Group|24115|5|Briefly described|p2, p3 Fig.3|||Unconformably underlies the Collier Group to the east. Correlated with the Edmund Group. Geological Province: Edmund Basin.||||||
16679|Scorpion Group|24390|5|Briefly described|p12 Table 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Officer Basin.||||||
16679|Scorpion Group|24535|5|Briefly described|p2, 5|||Thickness: 10 km. Carbonate to fine to coarse clastic rocks. Unconformably underlies Collier Group. Correlated with Edmund Group.||||||26-NOV-13
16679|Scorpion Group|24578|4|Described|p776 Fig.1, p778 Fig.3|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Age: ~1600 Ma. Geological Province: Edmund and Collier Basins.||||||
16679|Scorpion Group|35596|4|Described|p8|||||||||
16679|Scorpion Group|37460|3|Fully described|p157|||||||||
16679|Scorpion Group|37707|6|Mentioned|Fig.2|||||||||
16679|Scorpion Group|38243|6|Mentioned|Fig.2|||||||||
16679|Scorpion Group|38515|4|Described|p14|||||||||
16679|Scorpion Group|38516|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16679|Scorpion Group|38988|6|Mentioned|p8|||||||||
16679|Scorpion Group|40089|6|Mentioned|p56|||||||||
16679|Scorpion Group|40354|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16679|Scorpion Group|40355|4|Described|p8|||||||||
16679|Scorpion Group|40934|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
16679|Scorpion Group|40938|5|Briefly described|p4|||||||||
16679|Scorpion Group|43492|6|Mentioned|8|||||||||
16679|Scorpion Group|43595|6|Mentioned|Fig 3-43,p348|||Age: 1.2-1.6 Ga||||||
16679|Scorpion Group|44142|6|Mentioned|p309|||Of Bunting et al. (1982); here (Williams, 1990) designated a Subgroup of the Bangemall Group.||||||
16679|Scorpion Group|50085|5|Briefly described|p12 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Officer Basin.||||||
16679|Scorpion Group|50188|4|Described|p2 Fig. 1, p9, p12|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Supergroup. Possibly a correlative of Edmund Group. See also p2 Fig. 1.  Max. thickness:>2000m.  Age: 1600Ma. Geological Province: Bangemall Basin.||||||17-JUL-08
16679|Scorpion Group|50195|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Bangemall Supergroup. Includes the Millury and Willy Willy Formations, and Wonyulgunna Sandstone. Geological Province: Scorpion Basin.||||||11-APR-08
16679|Scorpion Group|50222|6|Mentioned|p319 Fig. 2, p334 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1.64Ga.||||||
16679|Scorpion Group|50226|5|Briefly described|p424 Fig. 5|||Of the Bangemall Supergroup.  Geological Province: Bangemall Basin.||||||
16679|Scorpion Group|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
16679|Scorpion Group|50334|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Supergroup. Geological Province: Bangemall Superbasin. Siltstone, sandstone, and dolomite.||||||11-JUN-04
16679|Scorpion Group|61023|5|Briefly described|p16 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Officer Basin.||||||11-APR-08
16679|Scorpion Group|61564|5|Briefly described|p589 Fig. 1, p590 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: ?1.6Ga. Geological Province: Edmund and Collier Basins.||||||07-NOV-08
16679|Scorpion Group|63866|5|Briefly described|p163, p168|||Bangemall Basin.||Bangemall Supergroup||||
16679|Scorpion Group|64283|5|Briefly described|p53|Paleoproterozoic|Paleoproterozoic|Dolomitic/sandy unit. May correlate with Quadrio Formation.||||||07-FEB-11
16679|Scorpion Group|64284|5|Briefly described|p58 Fig. 1|||Of the Bangemall Supergroup. Geological Province: Bangemall Basin.||||||07-FEB-11
16679|Scorpion Group|64285|5|Briefly described|p67 Fig. 2|||Of the Bangemall Supergroup. Geological Province: Bangemall Basin.||||||07-FEB-11
16679|Scorpion Group|64580|4|Described|map legend||Mesoproterozoic|Evaporitic and stromatolitic dolomite, and sandstone; lesser siltstone.||||||09-DEC-08
16679|Scorpion Group|64635|6|Mentioned|p2 Fig.1|||||||||
16679|Scorpion Group|64772|4|Described|p13, Plate 1, many Figs, App. 4|Mesoproterozoic|Mesoproterozoic|Includes Wonyulgunna Sandstone (previously of Collier Group), Willy Willy and Millury Formations and undivided Scorpion Group of evaporitic and stromatolitic dolomite, and sandstone; lesser siltstone.||Bangemall Supergroup||probable correlative of Edmund Group.||25-NOV-13
16679|Scorpion Group|65472|6|Mentioned|p5 Fig. 4|||Edmund Basin.||Bangemall Supergroup||||
16679|Scorpion 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.||||||
16679|Scorpion Group|66427|5|Briefly described|p41 Tb.1, p42-43, p47  |||Deposition began c.1.63 Ga, probably caused by Mangaroon Orogeny. Deformed <1.46-1.22 Ga with ?evaporite expulsion from Scorpion Diapir. Mildly deformed by Edmundian Orogeny.|ca. 1.63 Ga|Of the Bangemall Supergroup.||||
16679|Scorpion Group|67269|5|Briefly described|p20-21 Fig.19|Calymmian|Statherian|Bangemall Basin. Contains 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).|1797-1462 Ma.|||||
16679|Scorpion Group|68055|6|Mentioned|p76-77|||Bangemall Superbasin.||Bangemall Supergroup.||||
16679|Scorpion Group|68280|6|Mentioned|p26 fig 24|||Bangemall Basin.|1797-1462 Ma|||||
16679|Scorpion Group|69003|4|Described|vi,p4,p13 Fig.17,p15,p36,p41,p53,p72|Mesoproterozoic|Paleoproterozoic|Scorpion Basin, Capricorn Orogen. Possibly 10km thick. Includes clasts of deformed sedimentary rocks from the Earaheedy Basin. Deposition was probably coeval with lower Edmund Group.|< c.1650 Ma.||Wonyulgunna Sandstone.||A succession of sandstone, carbonate rocks, and evaporites.|
16679|Scorpion Group|69596|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||||||
16679|Scorpion Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Mesoproterozoic|Paleoproterozoic||1653-1455 Ma||||Evaporitic and stromatolitic dolomite and sandstone with lesser siltstone.|
16679|Scorpion Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Scorpion Basin. Deposited during the Capricorn Orogeny.||Bangemall Supergroup||||
16679|Scorpion Group|71158|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Scorpion Basin.|||Wonyulgunna Sandstone, Willy Willy Formation.|||
16679|Scorpion Group|71169|5|Briefly described|p71|Calymmian|Calymmian|West Australian Craton.|c. 1600-1500 Ma|||||
16679|Scorpion Group|71269|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen; West Australian Craton.||Unit of Bangemall Supergroup.|Includes Wonyulgunna Sandstone.|||
16679|Scorpion Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Millury Formation, Willy Willy Formation, Wonyulgunna Sandstone.|||
16679|Scorpion Group|72705|6|Mentioned|p3|||Capricorn Orogen.||||||
16682|Scotia Basalt|22534|4|Described|p9, p15|||||||||
16682|Scotia Basalt|42221|6|Mentioned|p7|||||||||
16682|Scotia Basalt|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
16682|Scotia Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
16682|Scotia Basalt|43102|6|Mentioned|p10|||||||||
16682|Scotia Basalt|43162|6|Mentioned|5|||||||||
16682|Scotia Basalt|43496|6|Mentioned|6|||||||||
16682|Scotia Basalt|60514|6|Mentioned|p65 Table 1|Archean|Archean|Overlain by Highway Ultramafics. Geological Province: Boorara Domain, Yilgarn Craton.||||||07-FEB-11
16682|Scotia Basalt|60627|6|Mentioned|p65 Tb.1|||||||||
16682|Scotia Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Boorara Domain. Kambalda Sequence.|||||Tholeiitic and high MgO basalt.|
16682|Scotia Basalt|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Boorara Domain. Tholeiitic and/or komatiitic basalt flows.||||||11-JUN-15
16682|Scotia Basalt|65834|6|Mentioned|p7, 33|||Boorara Domain, Kalgoorlie Terrane.||||Is overlain by Big Blow Chert.||
16682|Scotia Basalt|70326|5|Briefly described|p360,362,364-365|Neoarchean|Neoarchean|Geological province: Boorara Domain South, Kalgoorlie Terrane, Yilgarn Craton.||||Correlable to Lunnon Basalt.|Massive and pillowed basalt.|
16682|Scotia 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 Broad Arrow Subgroup.|||Basalt; pillowed to massive; metamorphosed; Komatiitic basalt; variolitic to pyroxene spinifex-textured; locally pillowed; metamorphosed.|
16682|Scotia Basalt|73391|5|Briefly described|p20, 177|||Boorara Domain, Eastern Goldfields Province. Occurs as a sliver on the W margin of the Scotia-Kanowna Dome and a thick succession on the E margin.||Lower Basalt.||Is truncated (unconformably overlain) by Panglo member. Equivalent to the Upper Basalt.|Poorly exposed mafic volcanics.|
16682|Scotia Basalt|73596|6|Mentioned|p1162|||Broad Arrow Inlier, Kalgoorlie Terrane.||Broad Arrow Subgroup.||Overlies Cock Robin Formation. Is overlain by Highway Formation.||
16720|Second Valley quartzite|37539|6|Mentioned|Fig.2|||||||||
16723|Secure Bay Monzogranite|23722|4|Described|p11|Proterozoic|Proterozoic|Replaces Secure Bay Adamellite.   Geological Province: Hooper Complex||||||
16723|Secure 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
16723|Secure Bay Monzogranite|42814|5|Briefly described|p8|||replaces Secure Bay Adamellite of Sofoulis et al (1971) and Gellatly and Sofoulis (1973).||||||
16723|Secure Bay Monzogranite|42815|5|Briefly described|map|||||||||
16723|Secure Bay Monzogranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
16723|Secure Bay Monzogranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
16723|Secure Bay Monzogranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv  and geochron files. Magmatic age of 1865+\-6 Ma (weighted mean 207Pb/206Pb).|1865+\-5 Ma (magmatic)|Unit of Paperbark Supersuite.|||Foliated, sparsely porphyritic, medium to fine grained biotite monzogranite with minor syenogranite and granodiorite; numerous shear zones and quartz veins|
16723|Secure Bay Monzogranite|72437|5|Briefly described|p62-63|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Monzogranite.|
16724|Sefton Greenstones|30440|6|Mentioned|p87|||Geochemistry||||||
16758|Septimus Limestone|13194|4|Described|p390 Tb. 4-16, p402 fig 4-66|Middle Tournaisian||Type Section: Mount Septimus 15o43'S 128o59'E. 25-300m thick marine shelf, shoreface and foreshore deposits.||Langfield Group||Overlies Enga Sandstone (conformably). Overlain by Zimmerman[n] Sandstone (conformably).|Limestone and sandy limestone; minor marl and calcareous sandstone.|19-JUL-16
16758|Septimus Limestone|13234|5|Briefly described|p252 |||Includes traces of oil.||||Correlated with the Ningbing Limestone.||
16758|Septimus Limestone|23820|5|Briefly described|p202 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
16758|Septimus Limestone|31519|6|Mentioned|p917|||||||||
16758|Septimus Limestone|31714|6|Mentioned|p32|||||||||
16758|Septimus Limestone|32648|6|Mentioned|p32|||Tournaisian||||||
16758|Septimus Limestone|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
16758|Septimus Limestone|32699|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Limestone, minor calcareous sandstone.||||||02-DEC-04
16758|Septimus Limestone|32701|4|Described|Table 2|||L.Carb. See p16.||||||30-NOV-06
16758|Septimus Limestone|32870|5|Briefly described|p46|||||||||
16758|Septimus Limestone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
16758|Septimus Limestone|34155|6|Mentioned|p94|||||||||
16758|Septimus Limestone|36257|6|Mentioned|Table 2.1|||||||||
16758|Septimus Limestone|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16758|Septimus Limestone|36551|6|Mentioned|Table 16|||||||||
16758|Septimus Limestone|36890|3|Fully described|p379|||Formerly Mount Septimus Limestone.||||||30-NOV-06
16758|Septimus Limestone|36904|5|Briefly described|p9|||||||||
16758|Septimus Limestone|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16758|Septimus Limestone|40494|4|Described|p17|||||||||
16758|Septimus Limestone|40792|6|Mentioned|p175|||||||||
16758|Septimus Limestone|40993|6|Mentioned|p10|||||||||
16758|Septimus Limestone|41712|6|Mentioned|Fig.14|||||||||
16758|Septimus Limestone|41839|4|Described|p28|||Formerly "Mount Septimus Limestone".||||||30-NOV-06
16758|Septimus Limestone|41864|3|Fully described|p108|||Formerly called "Mount Septimus Series", "Mount Septimus Limestone".||||||30-NOV-06
16758|Septimus Limestone|41865|5|Briefly described|Map legend||middle Tournaisian|||||||
16758|Septimus Limestone|42175|5|Briefly described|Fig.2 P200|||||||||
16758|Septimus Limestone|42547|4|Described|p101|||||||||
16758|Septimus Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
16758|Septimus Limestone|42994|6|Mentioned|p13|||||||||
16758|Septimus Limestone|43385|14|Not recorded|p176|||||||||
16758|Septimus Limestone|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
16758|Septimus Limestone|44965|14|Not recorded|Not recorded|||||||||
16758|Septimus Limestone|44993|14|Not recorded|p.7|||Camaratoechia.||||||
16758|Septimus Limestone|44994|6|Mentioned|p15|||Fig.6 Correlation.||||||
16758|Septimus Limestone|44998|14|Not recorded|App.3 p277-9|||Overlies Enga Sandstone.||||||
16758|Septimus Limestone|45015|6|Mentioned|p66|||Can be correlated with Moogooree Limestone. Geological Province: Bonaparte Gulf Basin.||||||01-JUN-06
16758|Septimus Limestone|45038|2|Defined|p.82||Early Carboniferous|See also Plates and Figures. L.Carb.||||||
16758|Septimus Limestone|45039|6|Mentioned|p1|||Lower Carboniferous. See also pp5,6,7,8,14 etc.||||||30-NOV-06
16758|Septimus Limestone|45050|6|Mentioned|p46|||See also pp50,51,57 etc. Late Tournaisian.||||||30-NOV-06
16758|Septimus Limestone|45063|6|Mentioned|p8|||See also pp18, 25 & Fig. 3. Tournaisian.||||||30-NOV-06
16758|Septimus Limestone|45097|6|Mentioned|Fig.|||Refers Mamet and Bedford (1968 p345).||||||30-NOV-06
16758|Septimus Limestone|45133|6|Mentioned|Fig.13|||||||||
16758|Septimus Limestone|45169|4|Described|p4|||||||||
16758|Septimus Limestone|46803|6|Mentioned|p147|||||||||
16758|Septimus Limestone|47040|6|Mentioned|Fig.3|||||||||
16758|Septimus Limestone|48635|14|Not recorded|Fig.1||Early Carboniferous|(D/52-10,11,14,15). Lower Carboniferous.||||||
16758|Septimus Limestone|48831|14|Not recorded|p.60|||||||||
16758|Septimus Limestone|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
16758|Septimus Limestone|48971|6|Mentioned|p15|||See also p31, p32, p35, p36, p37, p39, p40, p41.||||||30-NOV-06
16758|Septimus Limestone|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Of Langfield Group. Dolomitic and calcareous sandstone, minor limestone||||||22-JUL-04
16758|Septimus Limestone|60364|4|Described|p184, 187, 194|Tournaisian|Tournaisian|Of Langfield Gp. Overlies Enga Sst. Disconform.overlain by Zimmermann Sst and Border Creek Fm. Thickness at type section: 180m. Skeletal sandy calcarenite, and minor dolomitic quartz sandstone. Abundant brachiopods. Geological Province: Bonaparte Basin||||||30-NOV-06
16758|Septimus Limestone|60682|4|Described|p22 Table 5, 24|Tournaisian|Tournaisian|Of Langfield Group. Conformably overlies Enga Sandstone. Conformably overlain by Zimmerman Sandstone. Max. thickness: <100m. Dolomitic and calcareous sandstone. Geological Province: Bonaparte Basin.||||||11-MAY-05
16758|Septimus Limestone|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
16758|Septimus Limestone|64580|6|Mentioned|map legend|||Of Langfield Group.||||||15-DEC-08
16758|Septimus Limestone|64694|5|Briefly described|p233, p239, p247, p254 Fig.12|Tournaisian|Tournaisian|Burt Range Shelf, Onshore Bonaparte Basin.||Unit in Langfield Group.||Overlies Enga Sandstone. Is overlain disconformably by Zimmermann Sandstone.||
16758|Septimus Limestone|65331|5|Briefly described|Map legend|Tournasian|Tournasian|Of Langfield Group, Bonaparte Basin. Dolomitic and calcareous sandstone, minor limestone||||||
16758|Septimus Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Tournasian|||Langfield Group||||
16758|Septimus Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||
16758|Septimus Limestone|69452|3|Fully described|p36:6 Fig.36.5; 36:9, 12-14|Tournaisian|Tournaisian|Veevers and Roberts (1968). Equivalent to Mount Septimus Limestone of Noakes et al. (1952). Petrel Sub-basin, Bonaparte Basin. Type section at Mount Septimus where it is 300m thick; thins rapidly away from this area. Main outcrops in Burt Range (WA). High-energy shallow-marine deposits. Onshore.||Langfield Group.||Conformably overlies Enga Sandstone. Is overlain conformably by Zimmermann Sandstone, and unconformably by Keep Inlet and Milligans Formations.|Limestone, quartzose limestone and calcareous sandstone. The sparse NT exposures consist of thinly bedded fine-grained dolomitic and calcareous feldspathic sandstone. Diverse fossil assemblage.|12-JUL-16
16758|Septimus Limestone|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Unit of Langfield Group.||||
16758|Septimus Limestone|69673|5|Briefly described|p171, p179, p180|||300m thick. Potential as a reservoir rock.||Langfield Group|||Limestone, quartzose limestone and calcareous sandstone.|
16758|Septimus Limestone|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Langfield Group|||Dolomitic and calcareous sandstone, minor limestone.|
16758|Septimus Limestone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Dolomitic and calcareous sandstone, minor limestone|
16793|Shallow Shelf Carbonate|41217|5|Briefly described|Fig.2|||||||||
16794|Shamba Kappa Syenite|40811|4|Described|p320|||||||||
16806|Sharks Formation|30766|6|Mentioned|p7|||Subdivision of Warrawoona succession (Ingram, 1972)||||||
16806|Sharks Formation|37373|4|Described|p75|||||||||
16806|Sharks Formation|39697|6|Mentioned|p94|||||||||
16806|Sharks Formation|44150|6|Mentioned|p133 Tb.2-16|||East Pilbara. Of Ingram (1977). Probably obsolete; currently appears to be divided into Mount Ada Basalt, Duffer and Towers Formations.||||||
16830|Sherlock River complex|41594|6|Mentioned|p43|||||||||
16839|Shoal Reach Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24297|5|Briefly described|p4 Fig.3, p21|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Overlies Spencer Creek Formation. Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
16839|Shoal Reach Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
16839|Shoal Reach Formation|32307|6|Mentioned|p10|||Proterozoic||||||
16839|Shoal Reach Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
16839|Shoal Reach Formation|32660|5|Briefly described|Table 6|||||||||
16839|Shoal Reach Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Dolomite, sandy and silty; minor siltstone and intraformational breccia.||||||02-DEC-04
16839|Shoal Reach Formation|32700|4|Described|Table 1|||Lithology p14. Refers Randal (1962)||||||30-NOV-06
16839|Shoal Reach Formation|32701|4|Described|Table 1|||Auvergne Group. See p9.||||||30-NOV-06
16839|Shoal Reach Formation|32728|6|Mentioned|Fig.14|||||||||
16839|Shoal Reach Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
16839|Shoal Reach Formation|45112|4|Described|Table 15|||||||||
16839|Shoal Reach Formation|48938|2|Defined|p52|Proterozoic|Proterozoic|Measured section p98.||||||30-NOV-06
16839|Shoal Reach Formation|48942|3|Fully described|p71|||||||||
16839|Shoal Reach Formation|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Spencer Sandstone. Unconformably overlain by Bullo River Sandstone, Black Point Sandstone Member and Moonlight Valley Tillite.||||||21-JUL-04
16839|Shoal Reach Formation|60682|4|Described|p9 Table 2, 13|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Spencer Sandstone. Unconformably overlain by Bullo River Sandstone. Max. thickness: <110m.  Dolostone, dololutite, dolarenite, dolostone, sandstone, minor siltstone and shale. Geological Province: Victoria Basin.||||||30-NOV-06
16839|Shoal Reach Formation|60685|5|Briefly described|p4 Fig. 3, p2|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlain by the former Bardia Chert Member, which is now remapped as silcrete/duricrust. Geological Province: Victoria Basin.||||||17-JUN-13
16839|Shoal Reach Formation|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin.  Dolostone, sandstone, minor siltstone, and shale||||||
16839|Shoal Reach Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Spencer Sandstone.||
16839|Shoal Reach Formation|68733|5|Briefly described|p177 Fig.2, p183, p189 Fig.8|Cryogenian|Cryogenian|Victoria Basin.||Of the Auvergne Group.||Unconformably overlain by the Black Point Sandstone Member (Bullo River Sandstone).||06-DEC-17
16839|Shoal Reach Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Spencer Sandstone.||12-JUL-16
16839|Shoal Reach Formation|69441|5|Briefly described|p26:2-3, 5|Neoproterozoic|Neoproterozoic|Thickness <100m, thins to NE. Poorly exposed. Mixed carbonate/siliciclastic platform.||Auvergne Group.||Conformably (gradationally) overlies Spencer Sandstone.|Quartzose and silty dolostone, dololutite, dolarenite, dolostone, sandstone; minor siltstone and shale; local intraformational conglomerate.|12-JUL-16
16839|Shoal Reach Formation|69442|6|Mentioned|p27:1, 3 Tb.27.1|||||Auvergne Group.||Is overlain by Bullo River Sandstone, mostly dis/unconformably but gradationally at one location.||12-JUL-16
16839|Shoal Reach Formation|69673|5|Briefly described|p188|||100m thick.||Auvergne Group|||Quartzic and silty dolostone, dololutite, dolarenite, siltstone sandstone and intraformational conglomerate.|
16839|Shoal Reach Formation|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Silty and quartzic dolostone, dolostone, sandstone, minor siltstone and shale.|
16839|Shoal Reach Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
16839|Shoal Reach Formation|71302|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|Of Victoria Basin.||Unit of Auvergne Group.||Overlain unconformably by Black Point Sandstone Member. Underlain by Spencer Sandstone.||
16852|Sholl Creek Member|23529|6|Mentioned|p21|||Of the Wongawol Formation??   Max. thickness: ~1500m||||||
16852|Sholl Creek Member|31217|6|Mentioned|p42|||||||||
16852|Sholl Creek Member|37460|3|Fully described|p142|||||||||
16852|Sholl Creek Member|40355|6|Mentioned|p7|||||||||
16852|Sholl Creek Member|40938|4|Described|p57|||||||||
16869|Siberia Komatiite|22534|4|Described|p14, Fig.4 p7|||of Linger and Die Group. See also p20||||||
16869|Siberia Komatiite|22596|6|Mentioned|Fig.9 p419|||||||||
16869|Siberia Komatiite|22640|6|Mentioned|p298|||||||||
16869|Siberia Komatiite|23132|5|Briefly described|p336|||||||||
16869|Siberia Komatiite|42221|6|Mentioned|p9|||||||||
16869|Siberia Komatiite|42382|5|Briefly described|Fig.4 P11|||||||||
16869|Siberia Komatiite|42696|6|Mentioned|Plate 1B|||||||||
16869|Siberia Komatiite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
16869|Siberia Komatiite|42870|5|Briefly described|Table 1, P67|||||||||
16869|Siberia Komatiite|42989|5|Briefly described|Fig.2,Fig.4|||||||||
16869|Siberia Komatiite|43074|6|Mentioned|Fig.4|||||||||
16869|Siberia Komatiite|43101|5|Briefly described|Table 1.|||of Linger and Die Group||||||
16869|Siberia Komatiite|43102|5|Briefly described|p8|||||||||
16869|Siberia Komatiite|43162|6|Mentioned|5|||||||||
16869|Siberia Komatiite|43496|6|Mentioned|6|||||||||
16869|Siberia Komatiite|43574|6|Mentioned|Fig.1,p298|||||||||
16869|Siberia Komatiite|50551|5|Briefly described|p1094 Fig.5||Archean|In Eastern Goldfields Province.||||||07-NOV-08
16869|Siberia Komatiite|60076|5|Briefly described|p12 Tb. 2|||Max. thickness: <2600m.  Geological Province: Ora Banda domain.||||||
16869|Siberia Komatiite|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Of the Linger and Die Group. Overlain by Big Dick Basalt, underlain by Walter Williams Formation. Geological Province: Ora Banda Domain.||||||07-FEB-11
16869|Siberia Komatiite|60627|5|Briefly described|p65 Tb.1|||Of Linger and Die Group.||||||
16869|Siberia Komatiite|61849|5|Briefly described|p312|||Ultramafic flows that bound the northern margin of the Liberty Granodiorite pluton. Age is probably Archaean?||||||03-JUL-06
16869|Siberia Komatiite|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence.|||||Komatiite and high MgO basalt.|
16869|Siberia Komatiite|64771|5|Briefly described|p9|||Swager et al. (1995). Ghost Rocks area. Small patches of Cu mineralisation.|||||Coarsely spinifex-textured komatiite, locally foliated.|
16869|Siberia Komatiite|65204|5|Briefly described|pg6 Tbl.1, p9, p11, p12|Archean|Archean|Of Linger and Die Group. Is overlain by Big Dick Basalt. Metamorphosed; contains unusual gabbroic rocks, possibly due to extreme fractionation.||||||
16869|Siberia Komatiite|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.||Linger and Die Group.||||
16869|Siberia Komatiite|69631|5|Briefly described|p50-51|||Swager et al. (1995). Local small patches of copper mineralisation. Lithology described in some detail.||||Overlies Walter Williams Formation.|Coarsely spinifex-textured komatiite, foliated in places.|
16869|Siberia Komatiite|70326|5|Briefly described|p360,365|Neoarchean|Neoarchean|Geological province: Ora Banda region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Produced during ~2705 Ma komatiite eruption event.|~2705 Ma|||Overlain by Big Dick Basalt. Underlain by Walter Williams Formation.||
16869|Siberia Komatiite|70773|6|Mentioned|p50|||||||Overlies the Walter Williams Formation.|Spinifex textured komatiitic rocks.|
16869|Siberia Komatiite|71166|6|Mentioned|p9 fig 3.4a|||||||||
16869|Siberia 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 Vetters Subgroup.|||Komatiite and komatiitic basalt: commonly sepentinised or silicified, locally variolitic and/or pyroxene spinifex-textured; metamorphosed; ultramafic schist: includes talc-chlorite(-carbonate) and tremolite-chlorite schist|
16869|Siberia Komatiite|73391|5|Briefly described|p51, 53, 90, 173, 194, 244, 266, 279|||See also p330, Appendices. Ora Banda Domain, Kalgoorlie Terrane. 2800m thick.||Linger and Die Group.||Overlies Lower Basalt (?or Lindsays Basalt). Is overlain by the Big Dick Basalt, Mount Pleasant Sill and (unconformably) the Kurrawang Formation.|Olivine spinifex komatiite, spinifex textured high-Mg basalt.|
16869|Siberia Komatiite|73596|6|Mentioned|p1160|||Appears as Siberia Komatiite/Silver Lake Peridotite.||||||
16942|Sir Frederick Conglomerate|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
16942|Sir Frederick Conglomerate|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
16942|Sir Frederick Conglomerate|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
16942|Sir Frederick Conglomerate|24301|5|Briefly described|p17|||Geological Province: Amadeus Basin||||||
16942|Sir Frederick Conglomerate|33588|6|Mentioned|p6|||||||||
16942|Sir Frederick Conglomerate|34442|6|Mentioned|p7|||See also P8. Proterozoic. Equiv. Pertatataka Formation||||||
16942|Sir Frederick Conglomerate|35102|6|Mentioned|Fig.2|||||||||
16942|Sir Frederick Conglomerate|36551|6|Mentioned|Table 13|||||||||
16942|Sir Frederick Conglomerate|36887|5|Briefly described|p211|||||||||
16942|Sir Frederick Conglomerate|37928|6|Mentioned|Fig.4|||||||||
16942|Sir Frederick Conglomerate|39210|6|Mentioned|Fig.10|||||||||
16942|Sir Frederick Conglomerate|40740|6|Mentioned|p1|||||||||
16942|Sir Frederick Conglomerate|41852|6|Mentioned|p209|||||||||
16942|Sir Frederick Conglomerate|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Written as Sir Fred. Cong.  Conglomerate, sandstone.  Geological province: Amadeus Basin.||||||17-JUL-13
16942|Sir Frederick Conglomerate|43503|6|Mentioned|50|||||||||
16942|Sir Frederick Conglomerate|44109|5|Briefly described|p164|||Thick, poorly sorted conglomerate and boulder lenses, with clasts up 1m across. Geological Province: Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|44439|2|Defined|p.7,8, Tb.1, map|Cambrian|Neoproterozoic|U.Prot.-Cambrian. Age unclear. Lateral equiv.to Ellis Sandstone. Probably equiv.to Mt. Currie Conglomerate in NT (G52-1) (G52-2).||||||30-NOV-06
16942|Sir Frederick Conglomerate|44440|14|Not recorded|map legend|Cambrian|Neoproterozoic|Upper Proterozoic-Cambrian.||||||
16942|Sir Frederick Conglomerate|44499|14|Not recorded|opp.p.6, Tb.1|Early Paleozoic|Proterozoic|Proterozoic to Lower Palaeozoic.||||||07-NOV-08
16942|Sir Frederick Conglomerate|45041|4|Described|p39|||Proterozoic. Equiv. Winnall Beds||||||
16942|Sir Frederick Conglomerate|48842|2|Defined|p15-16|Early Paleozoic|Neoproterozoic|p.8,17,18,21,27,32,Pl.5,7,8. Tb.I. Conformably overlain by Maurice Formation; lenses into Ellis Sandstone. Sequence of pebble, cobble and boulder conglomerate with kaolinitic sandstone matrix and thin beds and lenses of sandstone and pebbly sandstone.||||||07-NOV-08
16942|Sir Frederick Conglomerate|48864|14|Not recorded|Tb.1.,p.10,Pl.10||Cambrian|(G52-2).||||||
16942|Sir Frederick Conglomerate|48963|6|Mentioned|Fig.2|||||||||
16942|Sir Frederick Conglomerate|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
16942|Sir Frederick Conglomerate|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Conglomerate, some sandstone. Underlies: Maurice Formation. Overlies: Carnegie Formation.||||||14-AUG-06
16942|Sir Frederick Conglomerate|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Conglomerate, some sandstone.||||||
16942|Sir Frederick Conglomerate|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
16942|Sir Frederick Conglomerate|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
16942|Sir Frederick Conglomerate|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
16942|Sir Frederick Conglomerate|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Is overlain by Maurice Formation.||
16942|Sir Frederick Conglomerate|67856|4|Described|p340 tab 4-8, p338, 337, 339, 344, 345|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. ~1200m thick. Type sction: Gillespie Hills 24o16'S, 124o42'E.||||Conformably overlain by Maurice Formation. Interfingers with and equivalent to Ellis Sandstone, also equivalent to Winnall beds. Unconformably overlies Carnegie Formation.|Piedmont conglomerate. Boulder, cobble and pebble conglomerate; sandstone lenses, quartz phenoclasts of silicified sandstone; metaquartzite and mica schist.|
16942|Sir Frederick Conglomerate|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin. Appears as Sir Fred Conglomerate on p683.||||Overlain by Mount Currie Conglomerate. Underlain by Boord Formation.||03-JUL-19
16942|Sir Frederick Conglomerate|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|69003|6|Mentioned|p60|Cambrian|Cambrian|W Amadeus Basin.||||||
16942|Sir Frederick Conglomerate|69031|5|Briefly described|p4, p9|||Amadeus Basin. Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Carnegie Formation. Is overlain by Maurice Formation.||
16942|Sir Frederick Conglomerate|69438|5|Briefly described|p23:2, 18, 20-21, 23|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||Overlies Carnegie Formation. Interfingers with Ellis Sandstone and is a correlative of (in part) Winnall beds. Is overlain by Maurice Formation.||12-JUL-16
16942|Sir Frederick Conglomerate|69606|5|Briefly described|p4 fig 2|Cambrian|Cambrian|Deposited during the Petermann Orogeny. Potential reservoir rock. Amadeus Basin.||||Overlies the Carnegie Formation, overlain by the Maurice Formation.|Sandstone and conglomerate.|
16942|Sir Frederick Conglomerate|69673|6|Mentioned|p64 fig 53|||||||Overlies Carnegie Formation, overlain by Maurice Formation||
16942|Sir Frederick Conglomerate|70416|6|Mentioned|p65 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin. Obsolete.||||||
16942|Sir Frederick Conglomerate|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)||||Cobble to boulder conglomerate; lesser interbedded sandstone.|
16942|Sir Frederick Conglomerate|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
16942|Sir Frederick Conglomerate|70839|4|Described|p329-333,335,337-340,345|Ediacaran|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Restricted to local depocentres, reaching estimated thicknesses of up to 2000m. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Concordant dates range between c. 1.06 and c. 2.7 Ga; two zircons older than c. 1.92 Ga. Dominant age component between c. 1.32 and c. 1.05 Ga, with minor components at c. 1.47, 1.57 and 1.76 Ga.|Max dep age: 1059+\-57 Ma (207Pb/206Pb)|||Overlain by Maurice Formation. Underlain by Carnegie Formation. Equivalent to Ellis Sandstone. Correlable to unit 2 of the Winnall beds.|Cobble and boulder conglomerate; clasts include quartzite, sandstone, and metasandstone lithologies.|
16942|Sir Frederick Conglomerate|71080|5|Briefly described|p30 fig 21|Cambrian||Amadeus Basin in WA. Supersequence 4.|||||Dominantly sandstone, some conglomerate.|
16942|Sir Frederick Conglomerate|71088|4|Described|p1-p2, p7-p8, p15, p17-p21, p24, p33|Neoproterozoic|Neoproterozoic|Restricted to the southern half of the Amadeus Basin. Reassigned to Supersequence 4. Potentially equivalent to the Ellis Sandstone. Correlated with the Pertatataka Formation by Wells et al., 1970; Grey, 1990 and Lindsay and Korsch., 1991. The dominant clasts of this unit are derived from the Dean Quartzite, Kulail Sandstone and Dixon Range beds.||||Overlain by the Maurice Formation. Unconformably overlain by the Mu Formation. Overlies the Carnegie Formation. Equivalent to the Winnall beds.|Clast-supported cobble to boulder conglomerate with well rounded clasts consisting of quartzite, sandstone and metasandstone.|
16942|Sir Frederick Conglomerate|71114|5|Briefly described|p170 fig 1b|Terreneuvian|Ediacaran|Appears (for reasons of space) as Sir Fred Cgl. SW Amadeus Basin.||||Shown as lateral equivalent to Ellis Sandstone, Mount Currie Conglomerate.||14-FEB-18
16942|Sir Frederick Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
16942|Sir Frederick Conglomerate|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)||||Sequence of pebble, cobble and boulder conglomerate with kaolinitic sandstone matrix and thin beds and lenses of sandstone and pebbly sandstone.|
16942|Sir Frederick Conglomerate|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
16942|Sir Frederick Conglomerate|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Carnegie Formation. Overlain by the Maurice Formation.|Lithic sandstone.|
16942|Sir Frederick Conglomerate|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Cobble to boulder conglomerate with predominantly sedimentary clasts and friable, sandy matrix; interbedded unit of red-brown, poorly sorted lithic sandstone in Mu Hills (inferred to have been deposited during the Petermann Orogeny).|
16942|Sir Frederick Conglomerate|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Ellis Sandstone.||
16942|Sir Frederick Conglomerate|71842|5|Briefly described|p2-3, p9|Early Cambrian|Ediacaran|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA).||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Ellis Sandstone. Correlable to Arumbera Sandstone or Winnall beds.||08-JAN-20
16942|Sir Frederick Conglomerate|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Cobble to boulder conglomerate; lesser interbedded sandstone.|
16942|Sir Frederick Conglomerate|72358|6|Mentioned|p118|Series 1|Ediacaran|Of Amadeus Basin.||||||
16967|Skerring kimberlite|41158|5|Briefly described|p6|||See also P25||||||
16968|Skewthorpe Formation|13194|6|Mentioned|p395 Tb. 4-16; p382,399 figs. 4-59, 4-63|Cambrian|Cambrian|Type Section: Hart Spring 15o19'S 128o27'E. 20-120m thick intertidal and subtidal system. All 4 Members found in Carlton Shelf.  [Note that the lat/long for the 4 Members do not look consistently correct].||Carlton Group||Overlies Hart Spring Sandstone. Overlain by Clark Sandstone (conformably) and Pretlove Sandstone (conformably).|Sandstone, siltstone, dolomitic sandstone and oolitic dolomite.|
16968|Skewthorpe Formation|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlies Hart Spring Sandstone. Overlain by Pretlove Sandstone.||06-OCT-16
16968|Skewthorpe Formation|24390|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin. Of the Carlton Group.||||||10-APR-08
16968|Skewthorpe Formation|31572|6|Mentioned|Fig.|||Correlation chart 1. Camb.||||||
16968|Skewthorpe Formation|32648|6|Mentioned|p32|||M-U.Cambrian||||||
16968|Skewthorpe Formation|32664|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Briefly described in notes||||||
16968|Skewthorpe Formation|32870|5|Briefly described|p39|||See also Fig.6||||||
16968|Skewthorpe Formation|36551|6|Mentioned|Table 16|||||||||
16968|Skewthorpe Formation|36890|3|Fully described|p375|||||||||
16968|Skewthorpe Formation|40301|6|Mentioned|p9|||||||||
16968|Skewthorpe Formation|40993|4|Described|p1|||||||||
16968|Skewthorpe Formation|41690|6|Mentioned|Fig.2|||||||||
16968|Skewthorpe Formation|41864|2|Defined|p38|Mindyallan|Boomerangian|||||||
16968|Skewthorpe Formation|41865|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|||||||
16968|Skewthorpe Formation|45012|14|Not recorded|p32,336|Late Cambrian|Middle Cambrian|late Middle Cambrian to Upper Cambrian fauna.||||||
16968|Skewthorpe Formation|45038|14|Not recorded|Fig 21,23,23,36||Cambrian|||||||
16968|Skewthorpe Formation|45058|6|Mentioned|Fig. 3|||See also Fig. 4||||||
16968|Skewthorpe Formation|48886|4|Described|p.38||Middle Cambrian|See also Figs & Plates. App.1, p.56, App.2, p.60. Middle Cambrian.||||||
16968|Skewthorpe Formation|49637|5|Briefly described|Fig. 6|Middle Cambrian|Middle Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||07-FEB-11
16968|Skewthorpe Formation|50085|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group.  Geological Province: Bonaparte Basin.||||||
16968|Skewthorpe Formation|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||10-APR-08
16968|Skewthorpe Formation|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
16968|Skewthorpe Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
16968|Skewthorpe Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
16968|Skewthorpe Formation|69437|5|Briefly described|p22:10-11|Series 4|Series 3|Bonaparte Basin, Centralian B Superbasin. Sequence 2.||Carlton Group.||Overlies Hart Spring Sandstone. Is overlain by Pretlove Sandstone.||12-JUL-16
16968|Skewthorpe Formation|69443|6|Mentioned|p28:21|||Bonaparte Basin.||||Correlated with Barkly Group.||12-JUL-16
16968|Skewthorpe Formation|69448|5|Briefly described|p33:7|||Bonaparte Basin.||Carlton Group.||Correlated with Overland Sandstone (Ord Basin).||12-JUL-16
16968|Skewthorpe Formation|69452|5|Briefly described|p36:5|Series 4|Series 3|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Conformably overlies Hart Spring Sandstone. Is overlain conformably by Pretlove Sandstone.||12-JUL-16
16968|Skewthorpe Formation|69573|6|Mentioned|p661|||Bonaparte Basin.||||||
16968|Skewthorpe Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
16968|Skewthorpe Formation|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian|||Carlton Group||Overlies Hart Spring Sandstone, overlain by Pretlove Sandstone||
16968|Skewthorpe Formation|71146|5|Briefly described|p6|Cambrian|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Hart Springs Sandstone. Overlain by the Pretlove Sandstone.|Carbonate and mudstone.|
17012|Smoke Hill Volcanics|24197|5|Briefly described|p98|Mesoproterozoic|Mesoproterozoic|Age: 1080Ma. Geological Province: Musgrave Block.||||||07-FEB-11
17012|Smoke Hill Volcanics|30386|4|Described|Table 1|||Proterozoic age. Table 1 on P6||||||
17012|Smoke Hill Volcanics|30388|6|Mentioned|p7|||Formerly Tollu Volcanics||||||
17012|Smoke Hill Volcanics|30390|4|Described|p55|||See also P56||||||
17012|Smoke Hill Volcanics|31967|6|Mentioned|p.4|||||||||
17012|Smoke Hill Volcanics|35323|6|Mentioned|p404|||||||||
17012|Smoke Hill Volcanics|43609|5|Briefly described|p14|||Dated 1078+/-5||||||
17012|Smoke Hill Volcanics|43693|5|Briefly described|p108|||||||||
17012|Smoke Hill Volcanics|43696|6|Mentioned|p45|||||||||
17012|Smoke Hill Volcanics|50607|6|Mentioned|p1.2, 3.1|Mesoproterozoic|Mesoproterozoic|Age: 1078 +/- 5Ma (SHRIMP). See also Smoke Hill volcanics.||||||19-SEP-13
17012|Smoke Hill Volcanics|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tollu Group. Age: 1075+/-5Ma. Correlated with the Puntitjata Rhyolite.||||||01-SEP-09
17012|Smoke Hill Volcanics|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Tollu Group. Underlain conformably by Mummawarrawarra Basalt. Consists of rhyolite and dacite.||||||15-JUL-08
17012|Smoke Hill Volcanics|63866|5|Briefly described|p207|Stenian|Stenian|Musgrave Province.|1078 +/- 5 Ma (Sun et al, 1996)|Bentley Supergroup||||
17012|Smoke Hill Volcanics|64722|5|Briefly described|p17|Stenian|Stenian||1078 +/- 5 Ma.|Of Tollu Group?||||11-APR-12
17012|Smoke Hill Volcanics|65135|5|Briefly described|p16|||Felsic lavas. Unconformably overlies Mummawarrawarra Basalt. Overlain by Hogarth Formation. Redefined in this paper to be part of the Tollu Group. Outcrops south of the Blackstone intrusion within the core of a syncline.||||||
17012|Smoke Hill Volcanics|65833|4|Described|p16|Stenian|Stenian|Of Tollu Group. Overlies Mummawarrawarra Basalt and Blackstone intrusion. Overlain by Hogarth Formation. Felsic lavas. Vitric dacite dated at 1026 +/- 26 Ma.||||||
17012|Smoke Hill Volcanics|65906|5|Briefly described|p2, p9, p19, p22-23, p29|Neoproterzoic|Mesoproterozoic|Series of rhyolite flows dated 1070 +/- 8 Ma and 1073 +/- 7 Ma (Pb/Pb crystallisation). A vitric dacite sample taken W of Mount Jane was dated 1026 +/- 26 Ma (U-Pb). Unconformably emplaced over the layered intrusions at Blackstone Range. Cut by microgranite veins dated 1070 +/- 5 Ma (Pb/Pb zircon). Underlies Hogarth Formation. The age of 1078 +/- 5 Ma by Glikson et al. (1996) is erroneous in that the sample dated was from a leucogranite vein/dyke.||||||
17012|Smoke Hill Volcanics|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Tollu Group.|||Felsic volcaniclastic conglomerate, silicified volcanic siltstone, porphyritic rhyolite and lesser dacite lavas and sills, felsic volcanic breccia sandstone, trachyte, granophyric granite.|
17012|Smoke Hill Volcanics|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Comprises the Tollu Group in this map area.||Unit in Tollu Group.|||Lavas, sills and cryptodomes of porphyritic rhyolite and lesser dacite; microcline phenocrysts to 6 mm; locally laminated, flow-banded, amygdaloidal or spherulitic.|
17012|Smoke Hill Volcanics|67128|4|Described|p5 Fig.3, p11, p13, p25, p27, p30|||Western Musgrave Province. Estimated thickness of 2km. A rhyolite thought to be of this unit was dated at 1078 +/- 5 Ma, but the present authors conclude it is a granite associated with NW-trending shear zones.|1026 +/- 26 Ma (dacite).|Tollu Group.||Overlies Mummawarrawarra Basalt and (probably) the Blackstone intrusion. Is overlain conformably by Hogarth Formation.|Felsic lavas, including rhyolite and plagioclase-phyric dacite; lesser trachyte. Local layers or lenses of volcaniclastic breccias, conglomerates, sandstones and tuffaceous siltstones.|
17012|Smoke Hill Volcanics|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Tollu Group.|||Porphyritic rhyolite and lesser dacite as lavas and subvolcanic sills and cryptodomes; includes up to 10% subhedral to euhedral microcline phenocrysts up to 6 mm; locally laminated, flow banded, amygdaloidal or spherulitic.|
17012|Smoke Hill Volcanics|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Mapped as 7 separate but un-named units.||Unit in Tollu Group.|||Felsic volcaniclastic conglomerate; silicified laminated volcanic siltstone; porphyritic rhyolite and lesser dacite as lavas, sills and cryptodomes; felsic volcanic breccia-sandstone, sandstone and conglomerate; granophyric granite.|
17012|Smoke Hill Volcanics|67375|4|Described|p19 Fig.11, p38, p40, p64, pp299-317.|Mesoproterozoic|Mesoproterozoic|Main exposure is in the east-trending Blackstone syncline. Felsic volcanic and volcaniclastic rocks; hosts hydrothermal vein systems and stratabound copper, lead, silver, zinc, gold and fluorite. It is most likely that the 1026 +/- 26 Ma dacite represents a subvolcanic sill that intruded into the Smoke Hill Volcanics (either belonging to the Hogarth Formation, or to an event that post-dates this formation).|1073 - 1026 +/- 26 Ma.|Unit in Tollu Group.||Intruded by Alcurra Dolerite.|Mainly porphyritic rhyolite and dacite lavas, sills and cryptodomes; volcaniclastics common, including breccia-sandstone and laminated sandstones to siltstones; some rheoignimbrites; locally flow-banded, amygdaloidal, spherulitic, hyaloclastic.|02-DEC-13
17012|Smoke Hill Volcanics|67553|3|Fully described|,95p20-21,38,40,42-43,64-65,85-86,89|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of  Blackstone Sub-basin, Bentley Sub-basin. Deposition of trachyandesites at 1073-1068 Ma (GSWA 171706), approximately coeval with emplacement/intrusion of Alcurra Dolerite. Locally folded, with mylonite zones that are either syn-or post-folding developed by 1071+\-8 Ma (Coleman, 2009) which may represent an effective minimum depositional age. Subvolcanic trachydacite sills emplaced near the base of the Smoke Hill Volcanics at 1026+\-26 Ma (GSWA 187177). Also intruded by Fe-rich olivine gabbros, olivine norites, ferronorites and ferrodiorites, hosting orthomagmatic nickel-copper mineralization at Nebo-Babel.|1073-1068 Ma|Unit of Tollu Group.||Lower unit of Tollu Group. Overlain by Hogarth Formation. Underlain by Mummawarrawarra Basalt/Kunmarnara Group.|Trachyandesites; felsic magmas.|
17012|Smoke Hill Volcanics|68100|5|Briefly described|p5, p26|Mesoproterozoic|Mesoproterozoic||1080-1030 Ma|Tollu Group|||Felsic volcanics, dacites.|
17012|Smoke Hill Volcanics|68995|6|Mentioned|p6, p8, p24, p31, p34, p45|||Blackstone Sub-basin. Overlies the G1 Blackstone intrusion. Ages are from GSWA 191728 (Coleman, 2009) and GSWA 189561 (CL Kirkland, 2013) respectively. Intruded in the Blackstone Basin by unnamed gabbros, norites, ferronorites, diorites and dolerites that are all equivalent to the Alcurra Dolerite. Misspelt as the Smoke Hill Rhyolite on p24. See also p49, p58, p64, p65.|1073 +/- 8 Ma - 1071 +/- 8 Ma|Tollu Group||Overlain by the Hogarth Formation.||
17012|Smoke Hill Volcanics|68996|5|Briefly described|p5, p32-33, p39, p41, p43|Mesoproterozoic|Mesoproterozoic||1078+/-3 Ma|Tollu Group||Overlain by Hogarth Formation.|Includes rhyolites, trachytes, granophyric granites. Granophyric granites with a median density of 2.64 g/cm^3, rhyolites with densities ranging from 2.67-2.7 g/cm^3 and trachytes with densitites of 2.77g/cm^3.|17-JAN-17
17012|Smoke Hill Volcanics|69091|4|Described|p73-74|||Blackstone Sub-basin. Crystallisation, or depositional, ages rhyolites: 1071 +/- 8 Ma (GSWA 191728, Coleman, 2009); 1073 +/- 7 Ma (GSWA 191706, Coleman, 2009) and 1073 +/- 8 Ma (GSWA 189561, Kirkland et al., in prep.)|1071 +/- 8 Ma, 1073 +/- 7 Ma, and 1073 +/- 8 Ma|Tollu Group||Is overlain by Hogarth Formation.|Rhyolites.|
17012|Smoke Hill Volcanics|69153|5|Briefly described|GEOL_LUT_CSV files;GA_geochron.csv; more|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Zircon (207Pb/206Pb) age of 1026+/-26 Ma (magmatic crystallization age, or, if zircons are inherited, then maximum crystallization age). See GEOCHRON/187177.1.pdf.||Tollu Group|||Felsic volcaniclastic conglomerate; volcanic siltstone; felsic volcanic (breccia-) sandstone; rheoignimbrite; feldspar-porphyritic dacite to rhyolite, granite, gabbro, and basalt; trachytic volcanic rocks; granophyric granite|02-SEP-14
17012|Smoke Hill Volcanics|69436|5|Briefly described|p21:14|||Blackstone Sub-basin [Bentley Basin]. Has been broadly correlated with Puntitjata Rhyolite based on their stratigraphic positions and geochronological ages. SHRIMP U-Pb age.|c.1073 Ma.|Tollu Group.||Unconformably overlies Mummawarrawarra Basalt. Is overlain by Hogarth Formation.||12-JUL-16
17012|Smoke Hill Volcanics|69655|5|Briefly described|p58|||Blackstone Sub-basin. Ages derived from GSWA records 191728 (Coleman, 2009) and 191706 (Coleman, 2009). An additional age of 1073 +/- 8 Ma from C, Kirkland 2014 (written comm) is provided.|1071 +/- 8 Ma and 1073 +/- 7 Ma||||Rhyolitic volcanic rocks.|
17012|Smoke Hill Volcanics|69729|5|Briefly described|p74 Fig.8, p80-81, p83|Mesoproterozoic|Mesoproterozoic|Talbot Sub-vasin. Shown as part of the Warakurna Supersuite. Geochemistry discussed. Appears also as Smoke Hills volcanics on p83.|c.1073-1071 Ma.|Tollu Group.||Is overlain conformably by Hogarth Formation.|Rhyolite.|
17012|Smoke Hill Volcanics|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age derived from dacite (187177.1.pdf)|1026 Ma - 1073 Ma (Inferred) 1026 Ma (SHRIMP)|Tollu Group||Overlain by Hogarth Formation|Trachytic, dacitic and acicular rhyolitic volcanic rocks with associated subvolcanic granophyre sills. Fine-medium grained granophyric granite; hornblende is acicular and up to 3cm in a granophyric groundmass; locally plagioclase is porphyritic.|
17012|Smoke Hill Volcanics|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 187177 (mesocratic dacite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum crystallisation age of 1026+\-26 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.|1073+\-7 Ma; 1026 Ma (inferred)|||Lowermost unit of Tollu Group. Overlain by Hogarth Fomation.|Trachytic, dacitic, and rhyolitic volcanic rocks with subvolcanic granophyre sills; rheoignimbrite; felsic volcanic breccia-sandstone and volcanic sandstone, volcaniclastic conglomerate, granophyric granite, silicified laminated volcanic siltstone.|
17012|Smoke Hill Volcanics|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Puntitjata Rhyolite was established by Close et al., 2003a.|c. 1073 Ma|Tollu Group||Equivalent to the Puntitjata Rhyolite.|Rhyolitic and dacitic volcanics.|
17012|Smoke Hill Volcanics|71211|6|Mentioned|p233|||Smoke Hill Felsic Volcanic also used p234.||Tollu Group|||Felsic lavas.|
17012|Smoke Hill Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite|
17012|Smoke Hill 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 187177 (mesocratic dacite) yielded a weighted mean 207Pb/206Pb age of 1026+\-26 Ma, interpreted as magmatic crystallisation age. 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.|1073+\-7 Ma; 1026 Ma (inferred)|||Lowermost unit of Tollu Group. Overlain by Hogarth Formation. Underlain unconformably by Giles Suite intrusions.|Dacitic to rhyolitic volcaniclastic rock; rheoignimbrite; Felsic volcanic breccia-sandstone, volcanic sandstone and volcaniclastic conglomerate; granophyric granite, porphyritic rhyolite and minor dacite lavas, volcaniclastic siltstone.|
17012|Smoke Hill Volcanics|71592|5|Briefly described|Appendix A.|||Musgrave Province. Magmatic age; U-Pb unspecified.|1520+/-250 Ma.|||||
17012|Smoke Hill Volcanics|72443|5|Briefly described|p744-746, p750-751, p753|||Blackstone sub-basin of the Bentley Basin. Geochemistry is discussed. Appears as the Smoke Hill Rhyolite on p751.||Tollu Group||Overlain by the Hogarth Formation.||
17079|Sokoman Iron Formation|41997|5|Briefly described|p79|||||||||
17115|South Kalgurli-Perseverance bed|33513|6|Mentioned|p30|||Rich gold mineralisation||||||
17128|South Perth Shale|12758|4|Described|p22, p3 Fig. 3|Neocomian|Neocomian|Of the Warnbro Group. Supersedes the South Perth Formation. Conformably overlies the Gage Sandstone. Max. thickness: 898m. Geological Province: Perth Basin.||||||22-JUL-09
17128|South Perth Shale|12759|3|Fully described|p34; p28 Tb. 7; p32 Fig 15.|Hauterivian|Valanginian|Defined Playford et al. (1976). Type section in South Perth No. 1 bore (AMG Zone 50, 391353 m E, 6460822 m N) between 498 m and 567 m depth.  Formerly included Gage Sandstone Member, which is raised to Formation status in this study. 300m thick. Overlain (conformably and transitionally) by Leederville Formation, and (unconformably) by Kings Park Formation.||Of Warnbro Group.||Overlies (unconformably) Cattamarra Coal Measures, Yarragadee or Parmelia Formations, and (conformably) Gage Formation. See Comments.|Thinly interbedded, grey to black siltstone and shale with minor thin, sandy beds and local thin, calcareous beds.|12-MAY-14
17128|South Perth Shale|14227|5|Briefly described|Enclos. 2|Early Cretaceous|Early Cretaceous|Of Warnbro Group.||||||07-FEB-11
17128|South Perth Shale|23279|5|Briefly described|p30|||||||||
17128|South Perth Shale|23816|4|Described|p246, 247|Neocomian|Neocomian|Geological Province: Perth Basin. Of the Wambro [Warnbro?] Group. Underlying unit: Yarragadee Formation. Overlying unit: Leederville Formation (conformable). Max. thickness: >795 m.||||||31-AUG-09
17128|South Perth Shale|24160|5|Briefly described|p94|Early Cretaceous|Early Cretaceous|Perth Basin.||Warnbro Group|||Grey and black shale and claystone, with sandstone at the base.|
17128|South Perth Shale|24443|5|Briefly described|Fig.31|Early Cretaceous|Early Cretaceous|Of Warnbro Group. Overlies Gage Sandstone. Overlain by Leederville Formation. Geological Province: Perth Basin.||||||
17128|South Perth Shale|29382|6|Mentioned|Table 10|||||||||
17128|South Perth Shale|29693|6|Mentioned|Fig.7|||||||||
17128|South Perth Shale|30188|2|Defined|p28|Early Cretaceous|Early Cretaceous|Refers Fairbridge(1953) (previously recorded as p74). Type section is in the South Perth No. 1 water bore (lat. 31deg 58' 31"S, long. 115deg 50' 57"E) between 497 m and 567 m (total depth). Reference section for whole Warnbro Group in Warnbro No.1 well between 1003 and 2204 m.||Warnbro Group||Leederville Fm overlies generally transitionally. Yarragadee Fm underlies unconformably.||15-AUG-18
17128|South Perth Shale|30217|6|Mentioned|p20|||Correlation. See also P24||||||
17128|South Perth Shale|31153|6|Mentioned|Fig. 57|||Stratigraphic table. Refers Cockbain & Playford (1973).||||||
17128|South Perth Shale|31562|5|Briefly described|p11|||||||||
17128|South Perth Shale|32471|6|Mentioned|p33|||||||||
17128|South Perth Shale|33044|4|Described|p44|||See also diags. 16 & 21 & maps 3 & 4||||||
17128|South Perth Shale|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
17128|South Perth Shale|35093|6|Mentioned|p22|||||||||
17128|South Perth Shale|35970|6|Mentioned|p77|||See also Table 12.||||||
17128|South Perth Shale|35983|6|Mentioned|Table 26|||||||||
17128|South Perth Shale|36257|6|Mentioned|Table 2.1|||||||||
17128|South Perth Shale|36265|5|Briefly described|Fig.3.26|Early Cretaceous|Early Cretaceous|Of the Warnbro Group. Geological province: Perth Basin.||||||28-JUL-09
17128|South Perth Shale|36293|2|Defined|p165|late Neocomian|late Neocomian|||||||
17128|South Perth Shale|36890|3|Fully described|p246|||Formerly South Perth Formation||||||
17128|South Perth Shale|37104|6|Mentioned|Fig.3|||||||||
17128|South Perth Shale|38221|6|Mentioned|Fig.4|||Perth Basin||||||
17128|South Perth Shale|38777|6|Mentioned|p30|||||||||
17128|South Perth Shale|38778|6|Mentioned|p15|||||||||
17128|South Perth Shale|39156|4|Described|p22|||||||||
17128|South Perth Shale|39211|6|Mentioned|p61|||Late Neocom. See also P62||||||
17128|South Perth Shale|39554|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17128|South Perth Shale|40349|6|Mentioned|p16|||||||||
17128|South Perth Shale|40395|6|Mentioned|p333|||||||||02-NOV-05
17128|South Perth Shale|40992|6|Mentioned|p11|||||||||
17128|South Perth Shale|41728|5|Briefly described|p444|||||||||
17128|South Perth Shale|41781|6|Mentioned|p11|||||||||
17128|South Perth Shale|41985|6|Mentioned|p65|||||||||
17128|South Perth Shale|41989|4|Described|p113|||||||||
17128|South Perth Shale|42075|6|Mentioned|p245|||||||||
17128|South Perth Shale|42194|4|Described|p61|||||||||
17128|South Perth Shale|43031|4|Described|p17,Fig.2.|||||||||
17128|South Perth Shale|43062|5|Briefly described|Table 2,p18|||||||||
17128|South Perth Shale|43096|5|Briefly described|Fig.2|||||||||
17128|South Perth Shale|43347|6|Mentioned|9|||||||||
17128|South Perth Shale|44144|4|Described|p504 Tb.4-21, p517|Hauterivian|Valanginian|Type Section: South Perth 1 bore: 31o59'S 115o51'E, 498-567 (TD) m.  795m thick shallow marine and paralic rocks.||Warnbro Group|Includes Gage Sandstone Member.|Overlies Parmelia Formation unconformably. Grades into overlying Leederville Formation.|Grey and black shale, claystone and siltstone, with sandstone (Gage Sandstone Member) at base.|
17128|South Perth Shale|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Of the Warnbro Group. Overlain by Leederville Formation. Underlain by Gage Sandstone.||||||07-FEB-11
17128|South Perth Shale|61811|5|Briefly described|p3 Fig.2. |Early Cretaceous|Early Cretaceous|Northern Perth Basin.||Unit in Warnbro Group.||Is overlain by Leederville Formation.||
17128|South Perth Shale|64580|6|Mentioned|map legend|||Of Warnbro Group.||||||
17128|South Perth Shale|64635|5|Briefly described|p4 Fig.3 |Hauterivian|Berriasian|||Unit in Warnbro Group.||Is overlain by Leederville Formation.||
17128|South Perth Shale|67115|6|Mentioned|p63, p64 Fig. 2, p65 Fig.3 |Cretaceous|Cretaceous|Lithology and trace elements detailed.||||Conformably underlies Mariginiup Member (Leederville Formation); overlies Gage Formation and unconformably overlies Yarragadee Formation.||
17128|South Perth Shale|67135|5|Briefly described|p5 Fig.7.|Cretaceous|Cretaceous|Perth Basin.||||Unconformably overlies Parmelia Formation. Is overlain by Leederville Formation.||
17128|South Perth Shale|67340|6|Mentioned|p6, 8, 25|Early Cretaceous|Early Cretaceous|Northern Perth Basin. Thermal rock properties.||||Unconformably overlies Parmelia Group. Is overlain by Leederville Formation.||
17128|South Perth Shale|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Barremian|Valanginian|||||Overlies the Gage Sandstone and unconformably overlies the Yarragadee Formation. Overlain by the Leederville Formation.||
17128|South Perth Shale|68254|6|Mentioned|p1036 Fg.2,p1037 Tb.2,p1040 Tb.3,p1042-4|Cretaceous|Cretaceous|See also South Perth Shale Formation.||||||
17128|South Perth Shale|68811|5|Briefly described|p92 fig 52, p180 tbl 39|Cretaceous|Cretaceous|||||Overlies the Yarragadee Formation and the Gage Formation. Overlain by the Leederville Formation.|Shale.|
17128|South Perth Shale|69081|5|Briefly described|p736 Tb.1|Early Cretaceous|Early Cretaceous|Geol. Prov: Perth Basin||Warnbro Group||overlies Gage Sandstone; is overlain by Leederville Formation; unconformably overlies Parmelia Group||
17128|South Perth Shale|69182|6|Mentioned|Ch2 p9, Ch2 p45,Ch2 p55, Ch2 p57|Lower Cretaceous|Lower Cretaceous|Perth Basin.||Warnbro Group||Unconformably overlies the Bunbury Basalt. Overlies the Gage Sandstone. Overlain by the Leederville Formation.||
17128|South Perth Shale|69297|6|Mentioned|p174, p175, p189|Barremian|Valanginian|Vlaming Sub-basin. Deposited in a marine or deltaic environment.||Warnbro Group||Overlies the Bunbury Basalt and the Gage Sandstone. Overlain by the Leederville Formation.||
17128|South Perth Shale|70097|5|Briefly described|p19 Fig.3|Aptian|Valanginian|Perth Basin. Mandurah Terrace, Vlaming Sub-basin and Dandaragan Trough.||Warnbro Group||Overlies Gage Sandstone (Parmelia Group) or Yarragadee Formation. Is overlain by Leederville Formation or Dandaragan Sandstone.|Shale.|12-SEP-17
17128|South Perth Shale|70099|5|Briefly described|Fig.4; p5|Barremian|Valanginian|Vlaming Sub-basin. Correlated to the Mentelle 5 syn-breakup Supersequence. Marine to deltaic.||Warnbro Group.||Overlies Gage Sandstone. Is overlain by Leederville Formation.||
17128|South Perth Shale|70128|5|Briefly described|p449, p451, p456, p458-462|Early Cretaceous|Early Cretaceous|Central Perth Basin. Modelled thickness distribution histogram.||Warnbro Group.||Conformably overlies Gage Sandstone. Is overlain conformably by Leederville Formation.||
17128|South Perth Shale|71377|5|Briefly described|p7, p9|Early Cretaceous|Early Cretaceous|Mandurah Terrace, Perth Basin.||Warnbro Group||Conformably overlain by the Leederville Formation.||
17128|South Perth Shale|71958|4|Described|p6-p7, p14, p16, p19, p35-p36|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin, Perth Basin.Named originally by Fairbridge (1953). A summary of the unit was outlined in Crostella and Backhouse (2000). Deposited in deltaic to shallow marine environments. Described as a good quality regional seal unit above the Gage Sandstone. This unit is relatively undeformed. Referred to as the South Perth Shale Formation on p88. See also p41, p51, p53-p54, p88, p119, p136, p162.||Warnbro Group||Overlies the Gage Sandstone. Overlain by the Leederville Formation.|Shallow marine shales and silts.|
17128|South Perth Shale|72258|5|Briefly described|p129|Early Cretaceous|Early Cretaceous|Of Perth Basin.||||Overlain by Leederville Formation. Underlain by Gage Sandstone.||
17137|Spargoville Formation|22534|6|Mentioned|p9|||||||||
17137|Spargoville Formation|23786|5|Briefly described|p3|||Of the Black Flag Beds? Geological Province: Yilgarn Craton||||||
17137|Spargoville Formation|24139|5|Briefly described|p238|Archean|Archean|Geological Province: Coolgardie Domain.  Of the Black Flag Beds.||||||07-NOV-08
17137|Spargoville Formation|24196|5|Briefly described|p47 Fig.5|||Unconformably overlain by Black Flag Formation. Unconformably overlies the Paringa Basalt. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||
17137|Spargoville Formation|42221|6|Mentioned|Table 1 P6|||||||||
17137|Spargoville Formation|42382|6|Mentioned|Table 1 P9|||||||||
17137|Spargoville Formation|42696|6|Mentioned|Plate 1B|||||||||
17137|Spargoville Formation|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
17137|Spargoville Formation|42892|5|Briefly described|p52, Fig.27|||||||||
17137|Spargoville Formation|43074|6|Mentioned|Table 1|||||||||
17137|Spargoville Formation|43162|6|Mentioned|5|||||||||
17137|Spargoville Formation|43496|6|Mentioned|6|||||||||
17137|Spargoville Formation|60514|5|Briefly described|p62, p64, p65 Table. 1, p66|Archean|Archean|Of the Black Flag Group. Coolgardie Domain. Finely bedded turbidites and  felsic sedimentary rocks. Geological Province: Yilgarn Craton.||||||07-FEB-11
17137|Spargoville Formation|60627|5|Briefly described|p62, p65 Tb.1|||Fine-grained felsic turbidites metamorphosed to schists, interbedded with tuffs. Of Black Flag Group.||||||
17137|Spargoville Formation|63981|6|Mentioned|p91, p93 Fig.3, |Archean|Archean|This name replaced (Hunter 1993) Black Flag Series (of Forman 1937).||Unit in Black Flag Group.||||
17137|Spargoville Formation|64633|6|Mentioned|p4 Fig.3, p6 Fig.4.|||Kalgoorlie Terrane.|2698 +/- 4 to 2686 +/- 3 Ma.|Unit in Kalgoorlie Sequence.|||Dacitic and rhyolitic volcanic rocks and minor intrusions.|
17137|Spargoville Formation|64893|5|Briefly described|p30|Archaean|Archaean|Age range: c.2698 to c.2666Ma. Overlies the Kambalda sequence in the kalgoorlie Terrane.||||||
17137|Spargoville Formation|65834|6|Mentioned|p7|||Coolgardie Domain, Kalgoorlie Terrane.||Black Flag Group.||||
17137|Spargoville Formation|66880|6|Mentioned|p8 Fig.2. |Archean|Archean|||||Unconformably overlies Paringa Basalt.||
17137|Spargoville Formation|67198|4|Described|p5 fig 2|Neoarchean|Neoarchean|Kalgoorlie Terrane. Age derived from volcaniclastics/tuff.|2686 +/- 3 Ma|Kalgoorlie Sequence||Overlies Paringa Basalt. Is overlain by White Flag Formation|Volcaniclastic rocks (rhyolite and dacite). Fine-grained turbidites.|11-SEP-17
17137|Spargoville Formation|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Kalgoorlie Sequence.||Overlain by White Flag Formation. Underlain by Paringa Basalt/Kambalda Sequence.|Felsic volcanic rocks and upper black shales.|
17137|Spargoville Formation|70482|6|Mentioned|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Age (U-Pb zircon) range from detrital zircons and intrusion.|2698-2687 Ma (Sircombe et al., 2007)..|Kambalda Sequence.|||Feldspar-rich volcanic sandstone, siltstone and lesser mudstone; high-Mg basalt; massive lavas and pillow basalt; varioles and amygdales also common.|
17137|Spargoville Formation|70773|5|Briefly described|p18 fig 11|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane.||Kalgoorlie Sequence||Overlies the Paringa Basalt. Overlain by the White Flag Formation.|Dacite and rhyolite.|
17137|Spargoville Formation|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.|2680 +/- 9 Ma.|||||
17137|Spargoville Formation|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Paringa Basalt. Overlain by the White Flag Formation.||
17137|Spargoville Formation|71308|5|Briefly described|p711 Fig.2|||Kalgoorlie Terrane.|2690 Ma.|Kalgoorlie Sequence.||||
17137|Spargoville Formation|71309|6|Mentioned|p740 Fig.3|||||||||
17137|Spargoville Formation|72049|6|Mentioned|p259-p260|||Kalgoorlie Terrane.||Black Flag Group||||
17137|Spargoville Formation|72485|6|Mentioned|p3 Fig.2|||||Kalgoorlie Sequence.||||
17137|Spargoville Formation|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
17137|Spargoville Formation|73391|4|Described|p19-21, 26, 50-51, 59, 108-109, 115-116|||See also p121, 132, 147, 178-181, 197, 199-203, 205-206, 208, 217, 231, 235-236, 238, 243, 246-247, 330, 441-442, Appendices. Informally named by Hunter (1993). Type section is at Widgiemooltha, the type locality may be near the Spargo's Reward gold mine 70km S of Kalgoorlie. Subsequently Krapez et al. (2000). Ora Banda, Kambalda Domains, Eastern Goldfields Province. Originally the Black Flag Series. Use for units well outside the type locality is not justified. Detailed DDH log. The Golden Mile Dolerite intrudes along the contact with the underlying Paringa Basalt.|2672 +/- 6 Ma (SHRIMP: Tripp, 2019)|Black Flag Group.||Overlies Victorious Basalt (Upper Basalt). Is overlain by Ballarat Conglomerate; grades upwards into White Flag Formation.|Felsic volcaniclastic and sedimentary rocks overlying the mafic and ultramafic successions throughout the Kalgoorlie district. Contains turbidite sedimentary rocks (wacke, mudstone), coherent flow-banded dacite lava. Graded beds.|
17139|Sparke Conglomerate|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
17139|Sparke Conglomerate|44231|5|Briefly described|Map Legend|Frasnian|Frasnian|Boulder, cobble and pebble conglomerate, poorly exposed; interbedded locally with Pillara Limestone, and Virgin Hills Formation. Geological Province: Canning Basin.||||||19-MAY-05
17139|Sparke Conglomerate|44366|14|Not recorded|p.20|||||||||
17139|Sparke Conglomerate|44403|2|Defined|p.12, opp.p.6, Tb.1||Famennian|E/51-12. Boulder to pebble conglomerate calcareous sandstone, torrential fanglomerate. Famennian. unconformably U/lain Pillara and Precambrian and interfingers with marine faunas of Mount Pierre Group. conformably O/lain by Mount Pierre Group.||||||
17139|Sparke Conglomerate|44404|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
17139|Sparke Conglomerate|44998|14|Not recorded|p.26,43, map.||Late Devonian|||||||
17139|Sparke Conglomerate|48826|14|Not recorded|Tb.III,p.19,20|||(E52-13).||||||
17139|Sparke Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
17139|Sparke Conglomerate|65486|6|Mentioned|p12|Devonian|Devonian|Canning Basin. Forms part of the Sparke Range. Low rainfall causes lack of tree cover.||||||
17139|Sparke Conglomerate|66127|3|Fully described|p69, pp127-133, pp146-149, p265 Fig.354|Famennian|Givetian|Of Guppy et al. (1958). Type area around Trig Stations J7 and J8 (Lawford Spring area). The conglomerate body around Virgin Hills, formerly included in this unit, is now placed in Bobs Bore Conglomerate. Southern Lennard Shelf. Forms the Sparke Range; at least 2 km thick. Mainly Precambrian clasts of quartzite, minor Devonian clasts. Includes an unnamed unit of sheared conglomerate, limestone and dolomite. Shown on Plates 4, 5, 7.|c.380 - 374 Ma.||Includes Galeru Member.|Locally lies between Gogo and Virgin Hills Formations. Interfingers with Pillara Limestone and early (Frasnian) Virgin Hills Formation.|Boulder, with lesser pebble, conglomerate, coarse- to fine-grained sandstone, with minor siltstone; alluvial-cone, fan-delta and submarine-fan deposits.|
17139|Sparke 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
17139|Sparke Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
17139|Sparke 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|
17146|Spearwood Sands|24464|5|Briefly described|p331|||||||||
17146|Spearwood Sands|37001|6|Mentioned|p28|||||||||
17150|Speewah Group|22547|4|Described|p21|Orosirian|Orosirian|Geological province: Speewah Basin. Previously part of Kimberley Basin, now redefined as Speewah Basin. Age: 1835- 1805 Ma. Thickness: 1500 m. Overlies Lamboo Complex, overlain by Kimberley Group||||||14-NOV-06
17150|Speewah Group|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1835Ma.||||||04-DEC-06
17150|Speewah Group|22754|4|Described|p10 Tb.2|Paleoproterozoic|Paleoproterozoic|Age: 1835-1830 Ma.||||||07-NOV-08
17150|Speewah Group|23125|5|Briefly described|Table.1|||||||||
17150|Speewah Group|23323|5|Briefly described|p455 Fig. 3, p456 Table 1|Orosirian|Orosirian|Age: 1834 +/- 3 Ma. In the Kimberley Craton/Western Zone.||||||07-FEB-07
17150|Speewah Group|23383|6|Mentioned|p18, p17|||Overlain by the Kimberley Group. Age 1834 Ma.  Geological Province: Speewah Basin.||||||25-JAN-05
17150|Speewah Group|23722|4|Described|p17|Proterozoic|Proterozoic|Early Proterozoic.   Thickness: 360m.   Geological Province: Kimberley Basin||||||
17150|Speewah Group|23751|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1835-1830 Ma (SHRIMP U-Pb). Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|24173|5|Briefly described|p19|||Of the Halls Creek Orogen. Felsic volcanics. Overlies Whitewater Volcanics. Geological Province: Speewah Basin. Age: 1834 +/- 3Ma (AGSO/OZCHRON).||||||06-APR-05
17150|Speewah Group|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, feldspathic sandstone, siltstone and mudstone; minor rhyolitic volcaniclastic sandstone. Age: c.1835Ma.  Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Clastic sedimentary rocks.  Age: c.1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
17150|Speewah Group|29380|6|Mentioned|p8|||||||||
17150|Speewah Group|29845|6|Mentioned|p113|||||||||
17150|Speewah Group|30097|6|Mentioned|Fig.54|||Also Tables 23,24,25||||||
17150|Speewah Group|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|30533|5|Briefly described|p15|||On Table 2. Age between Whitewater and Carson Volcanics.||||||
17150|Speewah Group|30558|6|Mentioned|p36|||||||||
17150|Speewah Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
17150|Speewah Group|30892|6|Mentioned|Table 1|||Carpentarian||||||
17150|Speewah Group|30893|5|Briefly described|p205|||Carpentarian. Lithology||||||
17150|Speewah Group|30894|4|Described|p249|||Carpentarian||||||
17150|Speewah Group|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|30896|4|Described|p13|||Carpentarian||||||
17150|Speewah Group|30897|6|Mentioned|p12|||Stratigraphy||||||
17150|Speewah Group|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17150|Speewah Group|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17150|Speewah Group|31393|6|Mentioned|Pl.25|||||||||
17150|Speewah Group|31404|6|Mentioned|p257|||||||||
17150|Speewah Group|31439|6|Mentioned|p293|||||||||
17150|Speewah Group|32108|6|Mentioned|p231|||||||||
17150|Speewah Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17150|Speewah Group|32660|4|Described|Table 3|||||||||
17150|Speewah Group|32663|6|Mentioned|p10|||||||||
17150|Speewah Group|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Mention in notes||||||
17150|Speewah Group|32728|6|Mentioned|Fig.3|||||||||
17150|Speewah Group|34137|6|Mentioned|p7|||||||||
17150|Speewah Group|34462|6|Mentioned|p8|||||||||
17150|Speewah Group|36003|6|Mentioned|p1028|||||||||
17150|Speewah Group|36551|6|Mentioned|Table 10|||||||||
17150|Speewah Group|36885|3|Fully described|p182|||||||||
17150|Speewah Group|36898|6|Mentioned|p183|||||||||
17150|Speewah Group|36902|6|Mentioned|p11|||||||||
17150|Speewah Group|37462|3|Fully described|p235|||||||||
17150|Speewah Group|38482|6|Mentioned|Table 1|||||||||
17150|Speewah Group|38988|6|Mentioned|Fig.4|||||||||
17150|Speewah Group|41158|6|Mentioned|p36|||See also p65.||||||04-DEC-06
17150|Speewah Group|41987|5|Briefly described|Fig.4 P74|||||||||
17150|Speewah Group|42149|5|Briefly described|Table 1 P709|||||||||
17150|Speewah Group|42710|5|Briefly described|map legend|Proterozoic||||||||
17150|Speewah Group|42811|4|Described|p20, Fig.5|||||||||
17150|Speewah Group|42814|4|Described|p12|||||||||
17150|Speewah Group|42815|5|Briefly described|map|Proterozoic||||||||
17150|Speewah Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
17150|Speewah Group|43561|6|Mentioned|p1437|||||||||
17150|Speewah Group|43595|5|Briefly described|p442|||||||||
17150|Speewah Group|43631|6|Mentioned|p10|||Kimberley region||||||
17150|Speewah Group|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
17150|Speewah Group|43853|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|43854|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
17150|Speewah Group|44140|4|Described|p293, p295-299, p304|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. ~1 km thick.|>1762 +/- 15 Ma (Rb-Sr).||O'Donnell, Tunganary  Formations; Valentine, Luman Siltstones; Lansdowne Arkose.|Unconformable on the Lamboo Complex and Hooper Complex (also faulted over the latter), and Whitewater Volcanics. Is overlain "subconformably" (?) by Kimberley Group. Is intruded by Hart Dolerite.|Quartzose & feldspathic arenite, interbedded with mudstone & minor amounts of acid volcanics; fluvial sands grade into fluvial and shallow-marine, then into deep-water silts.|08-MAR-18
17150|Speewah Group|44155|6|Mentioned|p236 Fig.3-35, p240, p241 Tb.3-4, p250|Paleoproterozoic|Paleoproterozoic|See also p252, p254 Fig.3-40.|||Includes O'Donnell Formation.|Overlies Whitewater Volcanics.||
17150|Speewah Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the O'Donnell and Tunganary Formations, Valentine Siltstone, Lansdowne Arkose, Luman Siltstone and Bedford Sandstone. Age: c.1835Ma. geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|44317|14|Not recorded|p.6||Carpentarian|||||||
17150|Speewah Group|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
17150|Speewah Group|44363|4|Described|p.3,7,8,9,12,13-28||Paleoproterozoic|Lower Proterozoic. units.||||||07-NOV-08
17150|Speewah Group|44364|14|Not recorded|map legend|||||||||
17150|Speewah Group|44366|14|Not recorded|p.11, Table 1||Carpentarian|||||||
17150|Speewah Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
17150|Speewah Group|44397|14|Not recorded|p.9,17,19, Table 2||Carpentarian|||||||
17150|Speewah Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
17150|Speewah Group|44868|5|Briefly described|Map Legend||Proterozoic|||||||
17150|Speewah Group|45047|5|Briefly described|p28|||See also p29.||||||04-DEC-06
17150|Speewah Group|48931|4|Described|p45|||||||||
17150|Speewah Group|48950|6|Mentioned|p36|||||||||
17150|Speewah Group|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Underlies the Kimberley Group unconformably and disconformably. Sedimentary rocks. Geological Province: Kimberley Basin.||||||07-NOV-08
17150|Speewah Group|50437|6|Mentioned|p4.1|||||||||
17150|Speewah Group|60533|5|Briefly described|p591, 592 Fig. 1, 593|Paleoproterozoic|Paleoproterozoic|Age: ca. 1835-1800Ma. Geological Province: Speewah Basin.||||||07-NOV-08
17150|Speewah Group|60714|6|Mentioned|p111|||Speewah Basin.|||Includes O'Donnell and Tunganary Formations, Valentine and Luman Siltstones, Landsdowne Arkose and Bedford Sandstone.|Unconformably overlies Hooper and Lamboo Complexes. Is intruded by Hart Dolerite. Is overlain unconformably by Kimberley Group.||
17150|Speewah Group|60724|5|Briefly described|p4, p5 Fig. 2|||Intruded by Hart Dolerite. Age: 1.83Ga.||||||
17150|Speewah Group|60844|5|Briefly described|pp15-16. |Late Paleoproterozoic|Late Paleoproterozoic|Speewah Basin. Exposed along the southeast and southwest margins of the Kimberley Region.|c.1835 - 1820 Ma.||Includes Bedford Sandstone.|Is overlain by Kimberley Group.||
17150|Speewah Group|63866|5|Briefly described|p127, p130, p133|||Western Zone, Halls Creek Orogen. Deposited in fluvial to shallow marine environments.|||Includes the Valentine Siltstone.|Unconformably overlies the Whitewater Volcanics. Disconformably overlain by the Kimberley Group. Intruded by the Hart Dolerite.|Pebbly conglomerate, sandstone and siltstone.|
17150|Speewah Group|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||||||
17150|Speewah Group|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, feldspathic sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic sandstone.||||||09-DEC-08
17150|Speewah Group|64724|5|Briefly described|p45, Fig.5|Orosirian|Orosirian|Deposited onto the Kimberley Craton at ~1835 Ma during the early stages of the Halls Creek Orogeny.||||||
17150|Speewah Group|64748|5|Briefly described|p268, p269 Fig 2, p278|Late Paleoproterozoic|Orosirian|Unconformity surface at the top of unit; intruded by Hart Dolerite; includes O'Donnell Formation, Tunganary Formation, Valentine Siltstone, Lansdowne Arkose, Lumen Siltstone, Bedford Sandstone.||||||
17150|Speewah Group|66845|4|Described|p536 Fig.2, p537|Paleoproterozoic|Paleoproterozoic|Felsic volcanic unit dates indicate this unit was deposited at 1834+/-3 Ma (Page et al. 1994)|c. 1835 Ma|||Unconformably overlies Western zone of Lamboo Complex and contiguous Hooper Complex; with Lamboo Complex, is overlain by Kimberley Group and its equivalents|Low-grade metasedimentary and metavolcanic rocks|21-JUL-15
17150|Speewah Group|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Western Zone of the Lamboo Complex.|||||Terriginous clastic rock.|
17150|Speewah Group|67563|5|Briefly described|p120 Fig.1|||Exposed as the lowest unit of the Kimberley Basin.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, and O'Donnell Formation.|Overlain by the Kimberley Group.||20-JAN-17
17150|Speewah Group|68078|4|Described|p1, p5, p8, p11, p14 figure 10, p17, p23|Paleoproterozoic|Paleoproterozoic|Age is from felsic volcanic unit within the group.|1835 +/- 3 Ma (SHRIMP)||Includes Valentine Siltstone, Bedford Sandstone, Lansdowne Arkose, Luman Siltstone, Tunganary Formation, O'Donnell Formation|Intruded by Hart Dolerite, unconformably/(disconformably?) overlain by Kimberley Group, unconformably overlies Marboo Formation, Whitewater Volcanics and Paperbark Supersuite|Felsic volcanic rocks, terriginous clastic rock. Formations within the group are comprised of quartz and lithic sandstone, feldspathic sandstone, arkose and interbedded siltstone.  Cross bedding present in sandstones. Around 1.5km thick on average.|13-SEP-22
17150|Speewah Group|68244|6|Mentioned|p661|||Mount House area, Kimberley region.||||||
17150|Speewah Group|68992|5|Briefly described|p498 Fig.1, p499|||Kimberley Basin.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, and O'Donnell Formation.|Unconformably underlain by the Hooper Complex and the Lamboo Complex. Overlain by the Kimberley Group.||
17150|Speewah Group|69003|5|Briefly described|p5, p18, p20|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Halls Creek Orogen.|||||Mainly interbedded siltstones and quartz, lithic, and feldspathic sandstones; minor volcanic and volcaniclastic rocks.|
17150|Speewah Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. ~1500m thick.|||Includes Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, O'Donnell Formation.||Sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic siltstone|21-JUL-15
17150|Speewah Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.|||Includes Bedford Sandstone, Luman siltstone, Lansdowne Arkose, Valentinte Siltstone, Tunganary Formation, O'Donnell Formation.||Undivided; sandstone, feldspathic sandstone, siltstone and mudstone; minor rhyolitic volcaniclastic sandstone.|
17150|Speewah Group|69435|6|Mentioned|p20:1|||Possible correlative of the Fitzmaurice Group.||||||12-JUL-16
17150|Speewah Group|69585|4|Described|p1-5, p7, p10-16, p27, p30-32|Orosirian|Orosirian|Overlies the western Lamboo Province; crops out along its eastern margin and west Kimberley. Fluvial and shallow-marine succession, deposited during and immediately after the 1835-1810 Ma Halls Creek Orogeny. Typically ~1.5km thick. The authors propose derivation largely from Paperbark Supersuite granites; deposition in a retro-arc foreland basin. Deformed during Yampi and King Leopold Orogenies. Age from Valentine Siltstone.|1835 +/- 3 Ma (Page and Sun, 1994).||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Unconformably overlies Whitewater Volcanics and Paperbark Supersuite. Is overlain unconformably by Kimberley Group. Is intruded by Hart Dolerite.|Dominantly fluvial quartz and lithic sandstone, feldspathic sandstone and arkose, with interbedded siltstone.|
17150|Speewah Group|69597|6|Mentioned|p3, p4, p5 fig 2b|||1.5 km thick. Unconformably deposited in the 1835 Ma Speewah Basin during the Halls Creek Orogeny.||||Overlain by the Kimberley Group. Intruded by the Hart Dolerite.||
17150|Speewah Group|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Speewah Basin. Thickness: 1500m. King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. 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 and geochron files.|1850-1784 Ma (Inferred)||Includes Lansdowne Arkose, Luman Siltstone, Tunganary Formation, Valentine Siltstone, Bedford Sandstone, O'Donnell Formation.|Overlain unconformably by Kimberley Group. Underlain unconformably by Hooper Complex, Lamboo Complex.|Undivided; sandstone, feldspathic sandstone, siltstone, and mudstone; minor rhyolitic volcaniclastic sandstone|
17150|Speewah Group|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.|||Includes O'Donnell and Tunganary Formations; Valentine and Luman Siltstones; Lansdowne Arkose.||Sandstone, siltstone, mudstone; minor conglomerate.|
17150|Speewah Group|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose.||Sandstones, siltstones, mudstones, arkose and conglomerate.|
17150|Speewah Group|70154|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 2_5m_geologyp98_lut.csv.|||Luman Siltstone, O'Donnell Formation, Lansdowne Arkose, Tunganary Formation, Valentine siltstone|||
17150|Speewah Group|70731|5|Briefly described|p268,270,272,274,276,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Siliciclastic sedimentary and minor felsic volcanic rocks. In contact with Whitewater Volcanics. Provenance from the SE and W basin margins dominated by Paleoproterozoic 1880-1850 Ma detrital zircons (Hollis et al., 2014). Difference in provenance and regional unconformity with overlying Kimberley Group reflect major change in basin-forming processes (extensional collapse of lithsphere following Halls Creek Orogeny; Hollis et al., 2014).||||Overlain unconformably by Kimberley Group/King Leopold Sandstone. Intruded by Hart Dolerite.||
17150|Speewah Group|70812|4|Described|p3, p6, p9, p19, p27, p30, p43|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. This unit features no mineral deposits; however, base metal mineralisation associated with felsic volcanism appears towards the base of this unit.|c. 1850-1800 Ma||Includes the o'Donnell Formation, Valentine Sandstone, Tunganary Formation, Luman Sandstone, Bedford Sandstone.|Overlies the Paperbark Supersuite. Unconformably overlain by the Kimberley Group.|Sandstones, siliciclastic sedimentary rocks and minor felsic volcanics.|
17150|Speewah Group|70826|6|Mentioned|p5 tbl 2, p9, p10|||Speewah Basin.||||Is intruded by the Hart Dolerite.||
17150|Speewah Group|70851|4|Described|p4-p6, p12, p16-p20, p24, p29|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geophysical response is discussed.|c. 1850-1800 Ma||Includes the O'Donnell Formation, Valentine Sandstone, Tunganary Formation, Luman Sandstone and the Bedford Sandstone.|Unconformably overlain by the King Leopold Sandstone. Intruded by the Hart Dolerite.||27-MAR-23
17150|Speewah Group|71113|5|Briefly described|p101-102,110|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Siliciclastic sedimentary rocks deposited on Western Zone rocks during Halls Creek Orogeny.||||Overlain unconformably by Kimberley Group.||
17150|Speewah Group|71140|6|Mentioned|p101-102, 110|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen. Deposited during the Halls Creek Orogeny.|||||Siliciclastic sedimentary rocks.|
17150|Speewah Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen, King Leopold Orogen. Of Speewah Basin. Thickness: 1500m. 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, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 1m_geologyl12_lut.csv and geochron files.|1835+\-3 to 1979 Ma (isotopic-inferred)||Includes Bedford Sandstone, Lansdowne Arkose, Luman Siltstone, O'Donnell Formation, Tunganary Formation, Valentine Siltstone.|Overlain unconformably by Kimberley Group.|Lithic and feldspathic sandstone, quartz sandstone, chloritic and micaceous siltstone, shale; minor rhyolitic ashstone and tuff|
17150|Speewah Group|71281|4|Described|p419, p421-423, p425, p429-432|Paleoproterozoic|Paleoproterozoic|Speewah Basin. 1.5km thick succession. Poorly outcropping. Represents a fluviatile to marine, transgressive and regressive event. Zircons are dominated by grains from the Paperbark Supersuite.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Unconformably overlies Whitewater Volcanics. Is overlain unconformably by the Kimberley Group. Is intruded by Hart Dolerite.|Predominantly low-grade metasedimentary siliciclastic rocks: conglomerates and rippled and cross-bedded fluviatile to marine deposits.|
17150|Speewah Group|71397|5|Briefly described|p5-6|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Mylonites on the margins of Speewah Group likely associated with c. 1000-800 Ma Yampi Orogeny (Tyler and Griffin, 1990; Tyler et al., 1995).||||||
17150|Speewah Group|71784|6|Mentioned|p83-84||Proterozoic|||||||
17150|Speewah Group|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||O'Donnell, Tunganary Formations; Valentine, Luman Siltstones; Lansdowne Arkose; Bedford Sandstone.|Is intruded by Hart Dolerite.||
17150|Speewah Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Speewah Basin.|Max age 1835+/-3 Ma, min ~1797 Ma.||||Sandstone, siltstone, and claystone; minor rhyolitic volcaniclastic siltstone.|
17150|Speewah Group|72437|5|Briefly described|P12, p113||||||Includes the Valentine Siltstone, O'Donnell Formation.||Contains a very minor component of felsic igneous rocks.|
17150|Speewah Group|72490|5|Briefly described|p1-6, p11, p13|Orosirian|Orosirian|Age is maximum age of deposition. Detrital zircons show a dominant ca. 1860 Ma age component that reflects derivation from the Paperbark Supersuite.|1814 +/- 10 Ma||Bedford Sandstone, Luman Siltstone, Lansdowne Arkose, Valentine Siltstone, Tunganary Formation, O'Donnell Formation|Intruded by Hart Dolerite.|Siliciclastic rocks.|
17150|Speewah Group|73255|6|Mentioned|p533 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
17153|Spencer Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24297|5|Briefly described|p4 Fig.3|||Of Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Lloyd Creek Formation; overlain by Shoal Reach Formation. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
17153|Spencer Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
17153|Spencer Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
17153|Spencer Sandstone|32660|5|Briefly described|Table 6|||||||||
17153|Spencer Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Quartz sandstone, silty sandstone, dolomitic sandstone.||||||02-DEC-04
17153|Spencer Sandstone|32700|4|Described|Table 1|||Lithology p14 Refers Randal (1962).||||||04-DEC-06
17153|Spencer Sandstone|32701|4|Described|Table 1|||Adelaidean. See p9. Of the Auvergne Group.||||||04-DEC-06
17153|Spencer Sandstone|32728|6|Mentioned|Fig.14|||||||||
17153|Spencer Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17153|Spencer Sandstone|45112|6|Mentioned|Table 6|||||||||
17153|Spencer Sandstone|48938|2|Defined|p50|Proterozoic|Proterozoic|Adelaidean? Measured section p97. See also p7.||||||04-DEC-06
17153|Spencer Sandstone|48942|3|Fully described|p71|||||||||
17153|Spencer Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Lloyd Creek Formation. Overlain by Shoal Reach Formation and unconformably overlain by Black Point Sandstone Member and Moonlight Valley Tillite.||||||21-JUL-04
17153|Spencer Sandstone|60682|4|Described|p9 Table 2, 10|Cryogenian|Cryogenian|Of Auvergne Group. Conformably overlies Lloyd Creek Formation. Conformably overlain by Shoal Reach Formation. Thickness: 140-170m. Quartz sandstone, silty sandstone, dolomitic sandstone. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Geological Province: Victoria Basin.||||||
17153|Spencer Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic|Of Auvergne Group, Victoria Basin. Quartz sandstone, silty sandstone, dolomitic sandstone||||||
17153|Spencer Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Ovelies Lloyd Creek Formation. Is overlain by Shoal Reach Formation.||
17153|Spencer Sandstone|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Quartz sandstone, silty sandstone, dolomitic sandstone.|
17153|Spencer Sandstone|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p185, p189 Fig.8|Cryogenian|Cryogenian|See also p192. Victoria Basin. Sm-Nd isotope data tabulated.||Of the Auvergne Group.||||06-DEC-17
17153|Spencer Sandstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Lloyd Creek Formation. Is overlain by Shoal Reach Formation.||12-JUL-16
17153|Spencer Sandstone|69441|5|Briefly described|p26:2-3, 5-6|Neoproterozoic|Neoproterozoic|Typically 140-165m thick. Shallow-marine with periods of subaerial exposure. Offset by Pinkerton Range Fault.||Auvergne Group.||Conformably overlies Lloyd Creek Formation. Is overlain conformably/gradationally by Shoal Reach Formation.|Basal thinly-bedded, fine- or medium-grained quartz sandstone; silty sandstone; dolomitic sandstone typical of upper part. Includes halite casts and pseudomorphs.|12-JUL-16
17153|Spencer Sandstone|69442|6|Mentioned|p27:3 Tb.27.1|||||Auvergne Group.||Is overlain unconformably by Big Knob beds and Bullo River Sandstone.||12-JUL-16
17153|Spencer Sandstone|69673|5|Briefly described|p188|||165m thick.||Auvergne Group|||Sandstone, siltstone and dolomitic sandstone.|
17153|Spencer Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Quartz sandstone, silty sandstone and dolomitic sandstone.|
17153|Spencer Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
17153|Spencer Sandstone|71302|4|Described|p1,6-7,65-75|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Exposed sporadically within a NE trending belt from the Pinkerton Range to the Victoria River Fault Zone on the  AUVERGNE 1:250 000 map sheet. Up to 165m thick. Probably deposited in a shallow-marine environment with periods of subaerial exposure (Dunster et al., 2000). Sample GA 1957135 (quartz sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1101+\-11 Ma, and is dominated by detritus in the range ca 1000-1250 Ma. Sample description, locality, zircon description, SHRIMP analyses and results are discussed.||Unit of Auvergne Group.||Overlain by Shoal Reach Formation. Underlain conformably by Lloyd Creek Formation.|Quartz sandstone, silty sandstone and dolomitic sandstone; thinly-bedded, fine- to medium-grained in the lower sequence, and typically more dolomitic to the top.|09-DEC-19
17163|Spielers Volcanics|30525|6|Mentioned|Map legend|Paleozoic|Adelaidean|Palaeozoic or Adelaidean Prob. Palaeozoic||||||07-NOV-08
17163|Spielers Volcanics|30533|4|Described|p21|||On Table 5 Age 357 m.y.||||||
17163|Spielers Volcanics|30895|6|Mentioned|Map legend|Paleozoic|Adelaidean|Adelaidean or Palaeozoic||||||07-NOV-08
17163|Spielers Volcanics|41158|6|Mentioned|p78|||||||||
17163|Spielers Volcanics|44155|5|Briefly described|p249 Tb.3-9|||750m thick.||||Conformably overlies Elimberrie Beds.|Quartz-feldspar porphyry, probably ash-flow tuff; foliated.|
17230|Square Top Microgranite|23722|4|Described|p13|Proterozoic|Proterozoic|Previously mapped as part of Whitewater Volcanics. Geological Province: Hooper Complex.||||||12-AUG-08
17230|Square Top Microgranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
17230|Square Top Microgranite|42814|5|Briefly described|p9|||Reserved as Square Top Metamicrogranite.||||||
17230|Square Top Microgranite|42815|5|Briefly described|map|||||||||
17230|Square Top Microgranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
17230|Square Top Microgranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
17230|Square Top Microgranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Metamorphosed altered quartz-phyric microgranite and quartz chloritoid kyanite rock|
17230|Square Top Microgranite|72437|5|Briefly described|p36|||Whole-rock analyses are provided.|||||Meta-monzogranite.|
17325|Steptoe Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
17325|Steptoe Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
17325|Steptoe Formation|23571|4|Described|p1, 10|Neoproterozoic|Neoproterozoic|Formerly known as the "Steptoe beds". Geological Province: Officer Basin. Underlying Unit: Kanpa Formation (conformable). Overlying Unit: Wahlgu Formation. Contains stromatolites.||||||12-MAY-05
17325|Steptoe Formation|24161|4|Described|p9 Fig.6, p13, p27|Neoproterozoic|Neoproterozoic|Conformably overlies the Kanpa Formation. Overlain by the Wahlgu Formation. Geological Province: Officer Basin.||||||
17325|Steptoe Formation|41751|6|Mentioned|p8|||||||||
17325|Steptoe Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.||Unit in Buldya Group.|||Sandstone, dolomite.|
17325|Steptoe Formation|61272|6|Mentioned|p123|||||||||
17325|Steptoe Formation|61732|5|Briefly described|p4 Fig. 3|Torrensian|Torrensian|Disconformable below Wahlgu Formation. Geological Province: central Officer Basin.  See also p131.||||||07-FEB-11
17325|Steptoe Formation|62453|3|Fully described|p5 Fig. 3, 22, 37, 52|Cryogenian|Cryogenian|Of the Buldya Group. Geological Province: Officer Basin. Underlies: Wahlgu Group, Lungkarta Formation. Overlies conformably: Kanpa Formation. Sandstone, dolomite and siltstone, some claystone and shale.||||||
17325|Steptoe Formation|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
17325|Steptoe Formation|63022|5|Briefly described|p1015|Neoproterozoic|Neoproterozoic|Top unit of the Buldya Group. Geological province: Officer Basin.||||||
17325|Steptoe Formation|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
17325|Steptoe Formation|64325|5|Briefly described|p80, p82 Fig. 2|Neoproterozoic|Neoproterozoic|A unit of Supersequence 1. Geological Province: western Officer Basin. Sandstone , dolomite, shale and minor evaporite deposits.||||||
17325|Steptoe Formation|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.||||||09-DEC-08
17325|Steptoe Formation|64793|6|Mentioned|p288|||The upper part of Supersequence 1 succession in Kanpa-1A, previously assigned to this unit, has now been included in Kanpa Formation (Carlsen et al, 1999).||||||
17325|Steptoe Formation|64970|5|Briefly described|p718, p719 Fig. 2, p721 Fig. 6, 6|Riphean|Riphean|Overlie Townsend Quartzite. Geological Province: Officer Basin.||||||27-MAY-09
17325|Steptoe Formation|65102|4|Described|p365,366,367,371; Figs 4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. 300-600m, sandstone, dolomite, shale & siltstone; eolian, inland playa; conformable on Kanpa Formation; type section in Kanpa 1A, 829-1301m; unfossiliferous.||||||
17325|Steptoe Formation|65363|6|Mentioned|p5 Fig.4. |Neoproterozoic|Neoproterozoic|||Unit in Buldya Group.||||
17325|Steptoe Formation|65365|5|Briefly described|p5, 7, 8 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group. Western and central Officer Basin.  Includes stromatolite assemblage.||||||19-MAR-12
17325|Steptoe Formation|65366|5|Briefly described|p23 Fig. 3, p24|Cryogenian|Cryogenian|Of Buldya Group, western and central Officer Basin.  Includes stromatolite assemblage.||||||
17325|Steptoe Formation|65410|6|Mentioned|p72, p78.|Neoproterozoic|Neoproterozoic|Western Officer Basin. Part of Supersequence 1. Contains a poorly preserved palynological assemblage, possibly similar to that in the Kanpa and Hussar Formations.||||||
17325|Steptoe Formation|65416|5|Briefly described|p137, p138 Fig.3, p141.|Late Proterozoic|Late Proterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Contains eolian sandstone; a potential reservoir.||||Conformably overlies Kanpa Formation. Is overlain unconformably by McFadden Formation.|Fine- to coarse-grained sandstone, dolomite, siltstone and shale.|
17325|Steptoe Formation|67195|4|Described|p9 fig 5, p10, p19 tbl 1, p44, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.76 W/mK. See also App 1, App 2.||||Overlies Kanpa Formation, Unconformably overlain by Table Hill Volcanics, Lupton Formation|Fine to medium grained sandstone interbedded with dolomite (some stylolites), shale and mudstone; laminated interbedded siltstone/sandstone.|
17325|Steptoe Formation|67200|5|Briefly described|app 2 p9||||||||Dolomite with claystone chips; sandstone.|
17325|Steptoe Formation|68270|5|Briefly described|p678|Cryogenian|Cryogenian|Western Officer Basin.||||Overlain disconformably by Wahlgu Formation (Karstified surface).||
17325|Steptoe Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
17325|Steptoe Formation|69029|6|Mentioned|p328-330|Neoproterozoic|Neoproterozoic|Of Officer Basin. Contains thin organic-rich source rock shales ranging from fair to good oil potental.||||Overlain unconformably by Lupton Formation or McFadden Formation or Wahlgu Formation. Underlain unconformably by Kanpa Formation.||
17325|Steptoe Formation|69091|5|Briefly described|p30 Fig.3.5, p38 Fig.3.7, see comments|Neoproterozoic|Neoproterozoic|Officer Basin. See also p41 Fig.3.8, p81 Fig.4.17, p174 Fig.9.5, p177 Fig.9.6, p200 Fig.10.2.||Buldya Group||||
17325|Steptoe Formation|69152|4|Described|500k_geologyp08_lut||Neoproterozoic|||Buldya Group|||Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.|07-AUG-15
17325|Steptoe Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian|||Buldya Group||||
17325|Steptoe Formation|70793|5|Briefly 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_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.||Unit of Buldya Group.||||
17325|Steptoe Formation|71268|5|Briefly described|100k_interpgeop_lut.csv|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.||Unit of Buldya Group.||||
17325|Steptoe Formation|71270|5|Briefly described|500k_interpgeop16_lut.csv|Tonian|Tonian|Of Officer Basin, Centralian Superbasin.||Unit of Buldya Group.||||
17337|Stirling Range Formation|22635|6|Mentioned|p482||Proterozoic|||||||
17337|Stirling Range Formation|22716|5|Briefly described|table4, p238|Mesoproterozoic|Mesoproterozoic|||||||
17337|Stirling Range Formation|22737|5|Briefly described|3,10,12-14,16|Proterozoic|Proterozoic|||||||
17337|Stirling Range Formation|23514|5|Briefly described|p102 Fig.1|Neoproterozoic|Neoproterozoic|||||||
17337|Stirling Range Formation|23727|5|Briefly described|p4 Fig 1.|||||||||
17337|Stirling Range Formation|23914|5|Briefly described|p143|Neoproterozoic|Neoproterozoic|Geological Province: Yilgarn Craton.||||||
17337|Stirling Range Formation|24160|6|Mentioned|p150, p151 Fig.76.|||Northern foreland of Albany-Fraser Orogen.||||||
17337|Stirling Range Formation|24526|6|Mentioned|p105 Fig. 6|Mesoproterozoic|Mesoproterozoic|Age is controversial: 1150Ma (Rb-Sr whole rock: Turek and Stephenson 1966) and 2000-1900Ma (zircon and monazite: Rasmussen et al 2002).  Geological Province: Yilgarn Craton.||||||
17337|Stirling Range Formation|24542|6|Mentioned|p2 Fig.2|Proterozoic|Proterozoic|||||||
17337|Stirling Range Formation|38578|4|Described|p20|||||||||
17337|Stirling Range Formation|38764|6|Mentioned|p109|||||||||
17337|Stirling Range Formation|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17337|Stirling Range Formation|41341|6|Mentioned|p8|||||||||
17337|Stirling Range Formation|42730|6|Mentioned|p16|||||||||
17337|Stirling Range Formation|42890|4|Described|p293|||||||||
17337|Stirling Range Formation|43012|5|Briefly described|p168|||||||||
17337|Stirling Range Formation|43030|5|Briefly described|Map Legend|||||||||
17337|Stirling Range Formation|43038|6|Mentioned|p9|||||||||
17337|Stirling Range Formation|43189|5|Briefly described|Map Legend||Proterozoic|||||||
17337|Stirling Range Formation|43212|5|Briefly described|p4||Neoproterozoic|Rb-Sr whole rock isochron of c.1150 Ma.but possible Ediacaran Fossils described from this unit.||||||10-DEC-09
17337|Stirling Range Formation|43697|6|Mentioned|p32|||||||||
17337|Stirling Range Formation|44137|5|Briefly described|p255-257|||> 1.6km thick. Fault-bounded; probably northward-directed thrust sequence. Whole-rock Rb-Sr isochron age of 1150 +/- 40 Ma (Turek and Stephenson, 1966) interpreted as age of deformation and metamorphism.|||||Lower and upper units of quartzite; a middle unit of quartzite, slate and phyllite.|
17337|Stirling Range Formation|60556|6|Mentioned|p2 Fig. 2|||||||||
17337|Stirling Range Formation|62093|6|Mentioned|p217|||||||||
17337|Stirling Range Formation|62381|5|Briefly described|p2 Fig.2.|||Northern Foreland, Albany-Fraser Orogen. 1600m-thick succession. Lower-greenschist facies metamorphism at 1215 +/- 20 Ma, possibly linked to dyke emplacement.|2016 +/- 6 Ma to 1800 +/- 14 Ma.|||Intruded by dolerite dykes aged 1218 +/- 3 Ma.|Quartzite, shale, slate, phyllite.|
17337|Stirling Range Formation|63866|5|Briefly described|p183-p185, p187, p197|||Northern Foreland.||||||
17337|Stirling Range Formation|64161|4|Described|p578-593|Orosirian|Orosirian|SHRIMP dating indicates maximum ages of 2016 +/- 6 Ma and minimum age of 1800 +/- 14 Ma. Possible equivalent of Woodline Formation.|||||Shallow marine succession >1600m thick consisting of quartzite, shale, slate and phyllite.|21-MAR-12
17337|Stirling Range Formation|64572|4|Described|p810-811, p811 Fig. 13|Ediacaran|Paleoproterozoic|Depositional age of 580-542Ma (Rb-Sr, Ediacaran). Succession of siliciclastic sedimentary rocks dominated by quartz sandstone, with minor shale. See p810-811 for more information.||||||10-FEB-14
17337|Stirling Range Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Metasandstone, quartzite, slate, and phyllite.||||||09-DEC-08
17337|Stirling Range Formation|64635|6|Mentioned|p2 Fig.1|||||||||
17337|Stirling Range Formation|64722|5|Briefly described|Fig. 2 p3-6, p17|Orosirian|Orosirian|Of Northern Foreland, Albany Fraser Orogen. Up to 1.6 km thick. Detrital xenotime grains give ages of 3460-1960 Ma; diagenetic xenotime gives an age of 1800 Ma.|||||Quartzite, slate and phyllite.|11-APR-12
17337|Stirling Range Formation|65357|5|Briefly described|p329-33, p330 Fig 1, p335-336|Statherian|Orosirian|~ 1.6 km thick; quartzite, shale, slate, phyllite. Max deposition age defined by ~2015 Ma detrital zircon. Min deposition age: 1800+/-14 Ma, derived from SHRIMP U-Pb dating of interpreted diagenetic xenotime overgrowths. Evidence of possible biota.||||||10-DEC-09
17337|Stirling Range Formation|65487|4|Described|p2, 11, 24, 23, 56-57; Figs. 1,12,27-28|Paleoproterozoic|Paleoproterozoic|100 km west of Mount Barren Group sediments. Sub-greenschist-lower greenschist facies quartzite, shale, slate and phyllite. Maximum depositional age of 2016 +/- 6 Ma (detrital zircons: Rasmussen et al., 2002,2004). Minimum age 1800 +/- 14 Ma (authigenic xenotime; Rasmussen et al., 2004). Interpreted as a shallow-marine tidal-dominated succession. Thrust faulted over the southern Yilgarn Craton by Albany-Fraser Orogeny.||||||
17337|Stirling Range Formation|67268|5|Briefly described|p4-5, p6, p16|Paleoproterozoic|Paleoproterozoic|Lies 100km west of Mount Barren Group. Relationship with Mount Barren Group uncertain (Spaggiari et al 2009)|c. 1800 +/-14 Ma, c.1206 +/- 6 Ma||||Quartzite, shale, slate and phyllite.|16-JUN-22
17337|Stirling Range Formation|67722|5|Briefly described|p5 fig 2.2, p7|Orosirian|Orosirian|Northern Foreland, Albany-Fraser Orogen. 1600 m thick succession. Max depositional age from detrital zircon. Minimum constraint on the time of deposition is provided by 1800 ¿ 14 Ma Pb-Pb ages for diagenetic xenotime. Metamorphic ages similar to intrusive dykes.|2016 +/- 6 Ma(SHRIMP) detrital zircons|||Intruded by dolerite dykes with c. 1220 Ma zirconolite ages.|Succession of deformed subgreenschist to greenschist facies quartzite, shale, slate and phyllite.|
17337|Stirling Range Formation|68186|5|Briefly described|p8, p13, p31|Paleoproterozoic|Paleoproterozoic|Muhling and Brakel (1985). Northern Foreland. Assigned to the newly-named Barren Basin, overlying the Yilgarn Craton. A shallow-marine, tide-dominated succession. Includes discoidal and trace-like fossils, previously thought to be Ediacaran. Maximum depositional age (detrital zircons and xenotime) and minimum age (authigenic xenotime) respectively (Rasmussen et al., 2002, 2004). Metamorphosed at 1215 +/- 20 Ma.|2016 +/- 6 Ma - 1800 +/- 14 Ma.||||Sub-greenschist to lower greenschist facies quartzite, shale, slate and phyllite.|
17337|Stirling Range Formation|68654|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Barren Basin.|c. 1800 Ma|||||
17337|Stirling Range Formation|69003|5|Briefly described|vi, p28, p30-31, p72|Paleoproterozoic|Paleoproterozoic|Barren Basin. Siliciclastic sediments, deposited on the S Yilgarn Craton after c.1800 Ma. Geochronology (U-Pb and diagenetic xenotime) described. Contains rare megascopic discoid fossils, interpreted as motile multicellular (or possibly syncytial) organisms; dated at 1800 +/- 14 Ma (U-Pb diagenetic xenotime).|c.1800 Ma.||||Dominantly shallow-marine to fluvial, mature, quartz-rich sandstones with interbedded siltstones and minor conglomerate.|
17337|Stirling Range Formation|69252|5|Briefly described|p7 Fig.3, p8-10, p23|||Northern Foreland, Albany-Fraser Orogen. A series of fault-bound, metasedimentary packages. c.1600m thick. Metamorphosed around 1215 +/- 20 Ma.|Deposition between 2016+/-6 Ma and 1800+/-14 Ma.||||Basal pink, fine-grained, well-sorted arenite, overlain by fine- and medium-grained quartz arenite interbedded with thin beds of slate and phyllite; gradationally overlain by light-coloured, medium-grained quartz arenite.|
17337|Stirling Range Formation|69595|4|Described|p3 fig 1, p8, p9 fig 5|Orosirian|Orosirian|Barren Basin, Albany Fraser Orogen. Deposited in a tidal dominated, shallow marine or fluival-deltaic setting. Maximum and minimum depositional ages.Contains discoidal and trace-like fossils. Older age given is a detrital zircon and xenotime age from Rasmussen et al, 2004. Younger age is a depositional age. Minimum 1600m thick. See also p11 tbl 2,  p12 fig 6,  p18, p19, p35, p37, p38, p39 fig 22.|2016 +/- 6 Ma - 1800 +/- 14 Ma - (||||Sub-greenschist to lower greenschist facies quartzite, shale, sandstone, slate and phyllite.|
17337|Stirling Range Formation|70023|6|Mentioned|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).||||||
17337|Stirling Range Formation|70085|6|Mentioned|p233-234|||Barren Basin, Western Albany-Fraser Orogen.||||||
17337|Stirling Range Formation|70090|4|Described|p442,444,446-447,453,456,458-459|Paleoproterozoic|Paleoproterozoic|Geological province: Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Thickness: >1600m. Deposited in a broad, relatively shallow basin under moderate to high-energy, fluvial to shallow marine environments. Metamorphosed to lower greenschist facies. Maximum depositional age: 2016+\-6 Ma. Minimum depositional age: 1800+\-14 Ma (Rasmussen et al., 2002, 2004), during Salmon Gums Event. Archean detrital zircon age populations include c. 3464, 2748, 2709 and 2656 Ma. Paleoproterozoic components includes c. 2246 and 2034 Ma. Similar detrital zircon pattern to Steere Formation.|c. 1800 Ma||||Qtz-rich sandstone, mudstone, shale.|
17337|Stirling Range Formation|70182|6|Mentioned|p4-5|Paleoproterozoic|Paleoproterozoic|Barren Basin, Albany-Fraser Orogen.|c.1815 Ma.|||||
17337|Stirling Range Formation|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
17337|Stirling Range Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, shale, slate, sandstone|
17337|Stirling Range Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Barren Basin.|||||Metasandstone, quartzite, slate, and phyllite.|
17337|Stirling Range Formation|72063|4|Described|p54-55,59,61-62|Orosirian|Orosirian|Geological province: Albany-Fraser Orogen. Thrust-bound sequence of metamorphosed (greenschist facies) siliciclastic sedimentary rocks within Albany-Fraser Orogen. Deposited in a shallow marine environment. Contains multiple horizons of discoidal and trace-like fossils on sandstone bedding surfaces. Deposited between  2.0 and 1.8 Ga (detrital zircons; Rasmussen et al., 2002 and diagenetic xenotime; Rasmussen et al., 2004). Metamorphism at ~1.2 Ga (monazite in sandstone, U-Th-Pb; Rasmussen et al., 2002). Coeval with amphibolite-grade metamorphism of Mount Barren Group (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). Hematite growth likely linked to late-stage orogenic uplift and gravity-driven infiltration of oxidising fluids.|c. 2.0-1.8 Ga||||Red (Fe-rich) sandstones and shales.|29-JAN-20
17337|Stirling Range Formation|72710|6|Mentioned|p4 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as SRF on p4 Fig.2. Shown as part of the Barren Basin.|1600 Ma to 1815 Ma.|||||
17337|Stirling Range Formation|73084|6|Mentioned|p12|||Yilgarn Craton and Albany-Fraser Orogen, Northern Foreland.||||||
17338|Stirling Sandstone|14019|3|Fully described|p6|||Of the Limbunya Group. Quartzarenite, sandstone, conglomerate. Unconformably overlies Inverway Metamorphics; disconformably overlain by Margery Formation. Type section 120m thick. Geological Province: Birrindudu Basin. Correlated with Masterton Sandstone.||||||
17338|Stirling Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Unconformably overlies Coomarie Sandstone and Hinde Dolostone; overlain by Margery Formation. Geological Province: Birrindudu Basin.||||||08-AUG-05
17338|Stirling Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|28255|6|Mentioned|p13, Tb. 11 (opp. p8)|||Of the Limbunya Group. Composed entirely of sandstone. Unconformable on Inverway Metamorphics and probably Bunda Grit also. Age is Adealidean or Carpentarian. Max. thickness: 120m.||||||
17338|Stirling Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
17338|Stirling Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  White and brown quartz sandstone, basal grit and minor conglomerate.  Overlies the Inverway Metamorphics unconformably; conformably underlies the Margery Formation.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
17338|Stirling Sandstone|32660|5|Briefly described|Table 6|||||||||
17338|Stirling Sandstone|33375|6|Mentioned|p9 Tb. 1|||Of the Limbunya Group. Age is Carpentarian or Adelaidean.||||||26-APR-05
17338|Stirling Sandstone|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17338|Stirling Sandstone|33378|5|Briefly described|Map legend|||Of the Limbunya Group. Age is Carpentarian or Adelaidean.||||||27-APR-05
17338|Stirling Sandstone|45112|6|Mentioned|p15|||||||||
17338|Stirling Sandstone|48943|2|Defined|p15|Proterozoic|Proterozoic|||||||
17338|Stirling Sandstone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Quartz arenite, dolomitic sandstone, conglomerate.  Unconformably overlies the Inverway Metamorphics.  Geological Province: Birrindudu Basin.||||||07-NOV-08
17338|Stirling Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
17338|Stirling Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Unconformably overlies Coomarie Sandstone and Hinde Dolostone. Is overlain by Margery Formation.||
17338|Stirling Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Is overlain by Margery Formation.|Quartz arenite, dolomitic sandstone, conglomerate (section only).|
17338|Stirling Sandstone|67479|5|Briefly described|p58|Orosirian|Orosirian|Maximum depositional age (LIMBUNYA; Carson, unpublished data) is similar to that of the Depot Creek Sandstone; implications mentioned.|c. 1830 Ma|||||24-JAN-17
17338|Stirling Sandstone|68733|5|Briefly described|p177-187, p193||Orosirian|Sweet et al. (1974). Birrindudu Basin. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1830 +/- 13 Ma|Basal unit of the Limbunya Group.||Unconformably overlies Inverway Metamorphics. Correlated with Mount Charles Formation.|Comprises predominantly coarse- to medium-grained well-rounded silicified quartz sandstone.|06-DEC-17
17338|Stirling Sandstone|69429|6|Mentioned|p14:2|||||Basal Limbunya Group.||Unconformably overlies Inverway Metamorphics.||12-JUL-16
17338|Stirling Sandstone|69432|4|Described|p17:2, 5-6, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 120m thick. Includes the former unit, the Bunda Grit, which was recognised as a facies variant of this unit; the name has been abandoned. Contains a synsedimentary fault-scarp conglomerate near its type section; activity on the Negri Fault was contemporaneous with deposition of the Sandstone. Detrital zircon maximum depositional age.|<1830 +/- 13 Ma (Carson, 2010).|Limbunya Group.||Unconformably overlies Inverway Metamorphics and Birrindudu Group.|Massive, thickly bedded, coarse quartz sandstone followed up-section by thinly to medium bedded, moderately sorted, medium to coarse quartz sandstone and minor thin conglomerate interbeds.|12-JUL-16
17338|Stirling Sandstone|69448|6|Mentioned|p33:8|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Contains evidence of a growth fault during deposition (the Negri Fault) which turned out to be long-lived, affecting Cambrian rocks in the overlying Ord Basin.||Limbunya Group.||||12-JUL-16
17338|Stirling Sandstone|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Unconformably overlies Coomarie Sandstone, Hinde Dolostone, overlain by Margery Formation||
17338|Stirling Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Section only.||Shown as base of Limbunya Group.|||Quartz arenite, dolomitic sandstone, conglomerate.|
17338|Stirling Sandstone|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Limbunya Group.|||Conglomerate: medium-thick bedded, cobble-pebbly, polymictic, cross-stratified; quartz sandstone: ripple marked, chert nodules; minor thin siltstone, mudstone.|
17338|Stirling Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
17338|Stirling Sandstone|71302|5|Briefly described|p6,72-74|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Reported maximum depositional age: 1830+\-13 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Almost entirely composed of zircon >1800 Ma in age, with significant populations of Neoarchean detritus at c. 2520 Ma, and contain small c > 1560-1640 Ma age populations. Carson (2013) suggested restricted provenance fromm the eastern zone of Halls Creek Orogen (c. 1910-1900 Ma mafic and felsic magmatism; see Blake et al., 2000). Tentatively correlated to Mount Charles Formation (of Cross and Crispe, 2007; see Carson 2013).||Unit of Limbunya Group.||Overlain by Margery Formation. Underlain by Coomarie Sandstone or Hinde Dolostone.||
17338|Stirling Sandstone|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1830+/-13 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
17338|Stirling Sandstone|72718|6|Mentioned|p7|Statherian|Orosirian|Birrindudu Basin.|younger than 1830 +/- 13 Ma|Limbunyah Group||Overlain by Margery Formation.||
17338|Stirling Sandstone|73083|6|Mentioned|p31-32|||Birrindudu Basin, lowest unit.|||||Clean quartz sandstone.|
17363|Stokes Siltstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Siltstone, shale, fossiliferous limestone.||||||
17363|Stokes Siltstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Middle Ordovocian|Geological province: Amadeus Basin.||||||07-FEB-11
17363|Stokes Siltstone|13995|5|Briefly described|p73, p75, p77, p89, p101, p103|Ordovician|Ordovician|Amadeus Basin. Contains Darriwilian bryozoans (the first in Australian successions), the brachiopod Dinorthis leviensis, and a rostroconch species. Contains Middle Ordovician pelecypods. Gastropod species, first decribed in the 1890s, are listed, but need reassessment. Contains the conodont Plectodina onychodenta, which has links to N China. Contains microvertebrate remains. May hold the oldest jawed vertebrate in the fossil record.||||Conformably overlies Stairway Sandstone. Is overlain conformably by Carmichael Sandstone.|Conglomerate, iron-rich dolomitised limestone, shallow subtidal mudstone.|
17363|Stokes Siltstone|22560|5|Briefly described|p5|Late Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22561|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|also see Stokes Formation p25||||||
17363|Stokes Siltstone|22565|5|Briefly described|p71 & Table 1||Ordovician|Thickness at Areyonga Creek measured from surface expression - 450m thick.  Approx. thickness measured from seismic data - 300m.||||||
17363|Stokes Siltstone|22566|5|Briefly described|p85|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22646|5|Briefly described|p105|Ordovician|Ordovician|also see Stokes Formation p107||||||
17363|Stokes Siltstone|22650|4|Described|p 160|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22651|6|Mentioned|Fig 10 btw p182-183|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22656|4|Described|p 279|Late Ordovician|Early Ordovician|||||||
17363|Stokes Siltstone|22761|6|Mentioned|Fig 2 on p351|Ordovician||Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22763|6|Mentioned|Table 1 on p386||Late Ordovician|Of the Larapinta Group..||||||04-DEC-06
17363|Stokes Siltstone|22804|6|Mentioned|Fig 2 on p432|Late Ordovician|Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|22806|6|Mentioned|p486|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|22825|6|Mentioned|p553|||||||||
17363|Stokes Siltstone|22826|6|Mentioned|p574|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|23361|5|Briefly described|16 Fig.4|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|23858|6|Mentioned|p914|||Overlain by Carmichael Sandstone. Geological Province: Amadeus Basin.||||||04-DEC-06
17363|Stokes Siltstone|24063|6|Mentioned|p222|||Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|24301|4|Described|p21, p7 Tb. 2|Ordovician|Ordovician|Of Larapinta Group. Previously combined with Carmichael Sandstone as "Stokes Formation" (Prichard and Quinlan, 1962). Overlies Stairway Sandstone, underlies Carmichael Sandstone. Max. thickness: 650m. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|29972|6|Mentioned|Table 1|||Upper Ordovician||||||
17363|Stokes Siltstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
17363|Stokes Siltstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group.||||||
17363|Stokes Siltstone|30544|6|Mentioned|p49|||||||||
17363|Stokes Siltstone|30615|6|Mentioned|p177|||Stratigraphic table - Palm Valley -2||||||
17363|Stokes Siltstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
17363|Stokes Siltstone|31707|4|Described|p53|||Lithology||||||
17363|Stokes Siltstone|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17363|Stokes Siltstone|32648|6|Mentioned|p32|||U.Ord.||||||
17363|Stokes Siltstone|32854|6|Mentioned|p352|||||||||
17363|Stokes Siltstone|33307|6|Mentioned|Fig.6|||||||||
17363|Stokes Siltstone|33738|6|Mentioned|Fig.5|||||||||
17363|Stokes Siltstone|33761|6|Mentioned|p146|||Ordovician. Larapinta Group||||||
17363|Stokes Siltstone|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See p15.||||||04-DEC-06
17363|Stokes Siltstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
17363|Stokes Siltstone|35102|6|Mentioned|Fig.2|||||||||
17363|Stokes Siltstone|36821|6|Mentioned|p398|||||||||
17363|Stokes Siltstone|36890|4|Described|p400|||Formerly Stokes Formation.||||||04-DEC-06
17363|Stokes Siltstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
17363|Stokes Siltstone|40128|6|Mentioned|p1|||||||||
17363|Stokes Siltstone|40136|5|Briefly described|p40|||||||||
17363|Stokes Siltstone|40740|3|Fully described|p55|||Mention p6.||||||04-DEC-06
17363|Stokes Siltstone|40810|4|Described|p11|||||||||
17363|Stokes Siltstone|41039|4|Described|p6|||||||||
17363|Stokes Siltstone|41224|6|Mentioned|p430|||Mention Fig.2||||||
17363|Stokes Siltstone|41621|5|Briefly described|Map legend|Late Ordovician||||||||
17363|Stokes Siltstone|41708|6|Mentioned|p206|||||||||
17363|Stokes Siltstone|41723|6|Mentioned|Map legend|Ordovician||||||||
17363|Stokes Siltstone|41819|6|Mentioned|Map legend|Late Ordovician||||||||
17363|Stokes Siltstone|41820|4|Described|p12|||||||||
17363|Stokes Siltstone|42037|5|Briefly described|Table 3 P79|||||||||
17363|Stokes Siltstone|42049|6|Mentioned|p220|||||||||
17363|Stokes Siltstone|42059|6|Mentioned|Fig.2 P131|||||||||
17363|Stokes Siltstone|42060|6|Mentioned|Fig.5 P140|||||||||
17363|Stokes Siltstone|42082|6|Mentioned|Fig.3 P323|||||||||
17363|Stokes Siltstone|42141|6|Mentioned|Fig.3 P570|||||||||
17363|Stokes Siltstone|42354|6|Mentioned|p6|||||||||
17363|Stokes Siltstone|42504|5|Briefly described|p77|||||||||
17363|Stokes Siltstone|42699|5|Briefly described|map legend|Ordovician||||||||
17363|Stokes Siltstone|42940|5|Briefly described|Plate 8|||||||||
17363|Stokes Siltstone|43035|5|Briefly described|p22|||Of Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|43225|5|Briefly described|Map Legend||Ordovician|Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|43503|6|Mentioned|11-50|Eastonian|Darriwilian|||||||
17363|Stokes Siltstone|43646|6|Mentioned|p553||Early Ordovician|||||||
17363|Stokes Siltstone|43647|6|Mentioned|p531|||||||||
17363|Stokes Siltstone|43649|5|Briefly described|Fig.1,p454-55,458|||Maybe misspelling of Stokes Formation||||||
17363|Stokes Siltstone|43803|6|Mentioned|Fig.5,p71|||||||||
17363|Stokes Siltstone|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
17363|Stokes Siltstone|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
17363|Stokes Siltstone|44395|14|Not recorded|p.9,12, Tb.2|||Upper Ordovician?||||||
17363|Stokes Siltstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
17363|Stokes Siltstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
17363|Stokes Siltstone|44484|14|Not recorded|p.11,12, Tb.1|Ordovician|Cambrian|Camb-Ord.||||||
17363|Stokes Siltstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44495|14|Not recorded|p.6, map||Ordovician|Ayers Rock sheet (G52-8).||||||
17363|Stokes Siltstone|44496|5|Briefly described|map legend||Ordovician|Shale and siltstone, some fossiliferous dolomite at base.||||||02-DEC-04
17363|Stokes Siltstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Camb-Ord.||||||
17363|Stokes Siltstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44499|14|Not recorded|opp.p.6, Tb.1||Ordovician|||||||
17363|Stokes Siltstone|44505|14|Not recorded|p.8,11, Table 1|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
17363|Stokes Siltstone|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian to Ordovician.||||||
17363|Stokes Siltstone|45041|2|Defined|p78|Middle Ordovician|Middle Ordovician|See also pp79-80. Of the Larapinta Group.||||||04-DEC-06
17363|Stokes Siltstone|45118|6|Mentioned|p1,3|||||||||
17363|Stokes Siltstone|45148|6|Mentioned|Fig.4|||Geol. prov: Amadeus Basin.||||||04-DEC-06
17363|Stokes Siltstone|45155|6|Mentioned|Fig.8|||||||||
17363|Stokes Siltstone|45170|6|Mentioned|Table 3|||||||||
17363|Stokes Siltstone|46928|6|Mentioned|Table 1|||||||||
17363|Stokes Siltstone|47052|6|Mentioned|p261|||||||||
17363|Stokes Siltstone|48963|6|Mentioned|Fig.3|||||||||
17363|Stokes Siltstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|50098|5|Briefly described|p1, p3 Fig. 2|Late Ordovician|Middle Ordovician|Of the Larapinta Group. Interbedded reddish and greenish shale and siltstone with thin beds of limestone. Max. thickness 650m. Geological Province: Amadeus Basin.||||||04-MAY-05
17363|Stokes Siltstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group.  Variegated siltstone; minor fine-grained silty sandstone and calc-arenite.  Geological Province: Amadeus Basin.||||||12-JAN-05
17363|Stokes Siltstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
17363|Stokes Siltstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, shale, limestone; fossiliferous. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|62376|5|Briefly described|p18|Late Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
17363|Stokes Siltstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
17363|Stokes Siltstone|62794|5|Briefly described|p288, p289 Fig.2.|Ordovician|Ordovician|Unit of Larapinta Group, overlying Stairway Sandstone and underlying Carmichael Sandstone.||||||
17363|Stokes Siltstone|62982|5|Briefly described|p7|Ordovician|Ordovician|Of the Larapinta Group. Overlies Stairway Sandstone; overlain by Carmichael Sandstone. Geological Province: Amadeus Basin.||||||16-JAN-07
17363|Stokes Siltstone|63562|6|Mentioned|p338 fig 3, p348, p352 fig 10|Late Ordovician|Early Ordovician|Of Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|64068|6|Mentioned|p77, 78, 226|||Of Amadeus Basin. Correlated with Carlo Sandstone, Mithaka Formation, Georgina Basin.||||||
17363|Stokes Siltstone|64334|5|Briefly described|p39-40, 42|Ordovician|Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain unconformably by Carmichael Sandstone.|Mudstones with carbonate interbeds.|
17363|Stokes Siltstone|64580|4|Described|map legend||Ordovician|Interbedded shale and siltstone; limestone; fine-grained sandstone.||||||09-DEC-08
17363|Stokes Siltstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Amadeus Basin.||||||
17363|Stokes Siltstone|64809|5|Briefly described|p2, p3 Fig.2, p11 Fig.10, p13 Fig.13 |Middle Ordovician|Middle Ordovician|Deposition on an open shelf in well-oxygenated waters.||||||
17363|Stokes Siltstone|65233|4|Described|p3 Fig. 2, p10|Late Ordovician|Early Ordovician|Of lower Larapinta Group. Gradational over Stairway Sandstone. Age: Middle Llanvirnian. Max. thickness: 650m. Geological province: Amadeus Basin.  Succession of fine clastics dominated by shale and siltstone with occasional evaporites.||||||07-FEB-11
17363|Stokes Siltstone|65256|6|Mentioned|p19|Ordovician|Ordovician|Of the Larapinta Group.||||||
17363|Stokes Siltstone|65449|5|Briefly described|p34-35||Darriwilian|Amadeus Basin. The lower part of this unit is correlated with Nita Formation on the basis of conodonts.||||Is overlain disconformably by Carmichael Sandstone. Time-correlative with Carribuddy Group and Worral Formation.||
17363|Stokes Siltstone|65489|5|Briefly described|p63, p125|Ordovician|Ordovician|Amadeus Basin. Could act as a caprock due to its low permeability.||Unit in Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|67326|5|Briefly described|p2|Late Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|67565|5|Briefly described|p41, p51. |Late Ordovician|Middle Ordovician|A recessive unit, outcropping poorly on valley floors. Up to 461 m thick. A seal in the Mereenie oil/gas field. Contains halite pseudomorphs, brachiopods and pelecypods.|||||Variegated siltstone, fine-grained grey silty sandstone, and grey-brown and orange-brown thinly-bedded and highly fossiliferous  limestone.|
17363|Stokes Siltstone|67856|4|Described|p338 fig 4-30, p347 tab 4-9, p337, p346|Late Ordovician|Middle Ordovician|Of Wells et al., 1964, 1970 etc. Type section: near Stokes Pass 23o35'S 132o07'E. Up to 650m thick (north Amadeus Basin) thinning southwards to 20-100m. Fossiliferous. Represents a variety of depositional environments, the upper part may be of high salinity.||Of Larapinta Group.||Unconformably overlain by Mereenie Sandstone (in WA), elsewhere conformably overlain by Carmichael Sandstone. Conformably overlies Stairway Sandstone or Proterozoic rocks.|Fossiliferous calcarenite. Red or green interbedded shale and siltstone; limestone interbeds; fine-grained sandstone.|
17363|Stokes Siltstone|68297|5|Briefly described|p177|Ordovician|Ordovician|Amadeus Basin. Includes disarticulated vertebrate fossils.||||Younger than Stairway Sandstone||
17363|Stokes Siltstone|68323|6|Mentioned|p4 Fig.2|Late Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
17363|Stokes Siltstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Amadeus Basin.||||Overlies Stairway Sandstone. Is overlain by Carmichael Sandstone.||12-JUL-16
17363|Stokes Siltstone|69438|3|Fully described|p23:2-3, 32, 36, 56-57, 60|Late Ordovician|Middle Ordovician|Redefined by Wells et al. (1970). Originally the Stokes Formation of Pritchard and Quinlan (1962). Was formerly mapped (Pritchard and Quinlan, 1962) as including rocks which were subsequently (Wells et al., 1970) assigned as a separate Formation (the Carmichael Sandstone). Type section is at Stokes Pass. Amadeus Basin. A recessive, valley forming unit, c.650m thick in the north-central part of the Basin, thinning southwards to 20m. Represents a range of depositional environments. Contains relatively few fossils (listed). Thick shales seal Stairway Sandstone reservoirs.||Larapinta Group.||Conformably and gradationally overlies Stairway Sandstone. Is overlain unconformably by Carmichael Sandstone.|A succession of interbedded shale and siltstone, with thin beds of silty-sandy limestone containing abundant fossil debris; red shale and lesser grey-green siltstone; and interbedded red to green shale, grey-green siltstone and fine sandstone.|12-JUL-16
17363|Stokes Siltstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
17363|Stokes Siltstone|69447|6|Mentioned|p32:5|||Amadeus Basin. Contains fossils with affinities to Hanson River beds (Wiso Basin).||||||12-JUL-16
17363|Stokes Siltstone|69449|6|Mentioned|p34:2 Fig.34.2|Ordovician|Ordovician|Eastern Amadeus Basin.||||||12-JUL-16
17363|Stokes Siltstone|69673|5|Briefly described|p64 fig 53, p66, p88, p89, p149 fig 120|Ordovician|Cambrian|650m thick. Deposited in shallow marine environment. Thick seal on the Stairway Sandstone.||Larapinta Group||Conformably overlies Stairway Sandstone, overlain by Carmichael Sandstone|Interbedded shale, sandstone and silstone, thin beds of fossiliferous limestone.|
17363|Stokes Siltstone|70793|4|Described|500k_interpgeop14_lut.csv|Late Ordovician|Middle Ordovician|Of Amadeus Basin (Phase 2). Events: Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|470-443.4 Ma (biostrat)||||Interbedded shale and siltstone; limestone; fine-grained sandstone|
17363|Stokes Siltstone|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Amadeus Basin.||||||
17363|Stokes Siltstone|71146|5|Briefly described|p6,  p43 fig 33|Late Ordovician|Middle Ordovician|Amadeus Basin.||Larapinta Group||Overlies the Stairway Sandstone.|Carbonate, mudstone and siltstone.|
17363|Stokes Siltstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
17363|Stokes Siltstone|71268|4|Described|GEOL_LUT_CSV files|Late Ordovician|Middle Ordovician|Of Amadeus Basin (Phase 2). Events: Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|470-443.4 Ma (biostrat)||||Interbedded shale and siltstone; limestone; fine-grained sandstone|
17363|Stokes Siltstone|71279|5|Briefly described|p355 Fig.2,p365,p370,p373-375,p382 Tb.1|Late Ordovician|Early Ordovician|Amadeus Basin. Linear magnetic anomalies discussed. Modelled magnetic properties.||Larapinta Group.||||
17363|Stokes Siltstone|71800|6|Mentioned|p26 fig 3|Late Ordovician|Middle Ordovician|Amadeus Basin.||||Overlies the Stairway Sandstone. Unconformably overlain by the Carmichael Sandstone.||
17363|Stokes Siltstone|72034|5|Briefly described|500k_interpgeop16_lut|Late Ordovician|Middle Ordovician|Amadeus Basin (Phase 2).  Age from biostratigraphy.|||||Interbedded shale and siltstone; limestone; fine-grained sandstone.|
17363|Stokes Siltstone|72369|4|Described|iii,p3-4,29,31-34|||Of Amadeus Basin. most poorly exposed unit of Larapinta Group, but laterally extensive. No previous geochronologcal constraint, however biostratigraphic age constraint provided by conodont macrofossils at early Gisbornian (460-456 Ma; Gibb et al 2009). LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND553 (micaceous siltstone) yielded an interpreted maximum depositional age of 493+\-5 Ma (youngest concordant zircon), but does not further constrain the age of the formation as it predates macrofossil age constraints at c. 460-456 Ma (e.g. Giss et al., 2008; Nicoll in Kennard et al 1986, Zhang et al 2003). Contains small groupings of Mesoproterozoic age zircon populations likely derived from Musgrave province. Paleoproterozoic to early Mesoproterozoic zircons (c. 2200-1475 Ma) may have been recycled from buried Cambrian and Neoproterozoic stratigraphy, or reflect input from proximal Aileron, Warumpi and Musgrave provinces, or distal east Gondwanan input. Cambrian zircon populations (c. 580-490 Ma) may have been derived from distal east Gondwanan input, as there are no known Cambrian sources proximal to Amadeus Basin. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Larapinta Group.||Overlain unconformably by Carmichael Sandstone. Underlain conformably by Stairway Sandstone.|Lower siltstone and limestone; sparsely fossiliferous succession, overlain by red and purple sandstone and shale.|18-DEC-19
17363|Stokes Siltstone|73085|6|Mentioned|p1|late Ordovician|early Ordovician|||||Underlain by Stairway Sandstone. Overlain by Carmichael Sandstone.||
17363|Stokes Siltstone|73119|6|Mentioned|p19|early Gisbornian|early Gisbornian|Age from Gibb et al. (2009).|460-456 Ma|||Conformably underlain by Stairway Sandstone.||
17363|Stokes Siltstone|73279|5|Briefly described|p3, p12|Ordovician|Ordovician|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group||Underlain by Stairway Sandstone. Overlain by Carmichael Sandstone.|Includes siltstone.|
17363|Stokes Siltstone|73346|6|Mentioned|p18|Late Ordovician|Darriwilian|Amadeus Basin. Includes the arandaspids Areyongalepis oervigi, Apedolepis tomlinsonae, and Sacabambaspis sp.||||||
17367|Stonewall Sandstone|22547|5|Briefly described|p24|||Of the Carr Boyd Group. Overlies Glenhill Formation, overlain by Pincombe Formation.||||||14-NOV-06
17367|Stonewall Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group.||||||
17367|Stonewall Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17367|Stonewall Sandstone|32660|5|Briefly described|Table 6|||||||||
17367|Stonewall Sandstone|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
17367|Stonewall Sandstone|32728|5|Briefly described|Table 6|||||||||
17367|Stonewall Sandstone|36551|6|Mentioned|Table 12|||||||||
17367|Stonewall Sandstone|36885|4|Described|p179|||||||||
17367|Stonewall Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
17367|Stonewall Sandstone|44155|5|Briefly described|p250 Tb.3-10|||300-450m thick.||Carr Boyd Group||Overlies Glenhill Formation unconformably or Kimberley Group unconformably. Is overlain gradationally by Pincombe Formation.|Subfriable medium- to coarse-grained quartz sandstone, subordinate argillaceous and feldspathic sandstone, granule sandstone, red shale.|
17367|Stonewall Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
17367|Stonewall Sandstone|44363|5|Briefly described|p.6,14,16,17|||(Adelaidean) Of theCarr Boyd Group.||||||04-DEC-06
17367|Stonewall Sandstone|44364|14|Not recorded|map legend|||||||||
17367|Stonewall Sandstone|45047|4|Described|p35|||Of the Carr Boyd Group.||||||17-OCT-12
17367|Stonewall Sandstone|45112|6|Mentioned|p34|||||||||
17367|Stonewall Sandstone|65417|5|Briefly described|pp156-159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Correlated with Lalngang Sandstone of the Fitzmaurice Group (NT). Braided-delta progradation and retreat.||Unit in Carr Boyd Group.||Conformably overlies Glenhill Formation. Is overlain conformably by Pincombe Formation.||
17367|Stonewall Sandstone|69435|5|Briefly described|p20:3|||Carr Boyd Basin. A previous correlation  with the Lalngang Sandstone (Fitzmaurice group, NT) is called into question.||Carr Boyd Group.||Overlies Glenhill Formation. Is overlain by Pincombe Formation.||12-JUL-16
17367|Stonewall Sandstone|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Pincombe Formation, overlies Glenhill Formation||
17367|Stonewall Sandstone|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, feldspathic sandstone, shale|
17389|Stottid Formation|37735|6|Mentioned|p18|||||||||
17454|Stubb Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
17454|Stubb Formation|22547|6|Mentioned|Fig4,p25|||Geological province:  Victoria River Basin. Overlies Wondoan Hill Formation.||||||05-DEC-06
17454|Stubb Formation|23937|5|Briefly described|p76 App. 1|||Of the Auvergne Group?||||||03-NOV-04
17454|Stubb Formation|24122|3|Fully described|p8, p5 Tb.1|Proterozoic|Proterozoic|Of Tijunna Group. Conformably overlies Wondoan Hill Formation. Originally included in the Auvergne Group.  Max. thickness: 210m.  Geological Province: Victoria Basin.||||||
17454|Stubb Formation|24297|3|Fully described|p15|Mesoproterozoic|Mesoproterozoic|Of Tijunna Group. Conformably overlies Wondoan Hill Formation. Was included in Auvergne Group on the 1st edition of VICTORIA RIVER DOWNS 1:250k. Maximum thickness: 115m.  Geol. Prov:  Victoria Basin.  See also p5 Tb. 2.||||||05-DEC-06
17454|Stubb Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Siltstone, shale, minor sandstone.||||||05-DEC-06
17454|Stubb Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group.   Geological Province: Victoria Basin||||||14-MAR-18
17454|Stubb Formation|24441|5|Briefly described|p1 Fig. 1, Appendix 2-1:2|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Overlies Wondoan Hill Formation; unconformably overlain by Jasper Gorge Sandstone. Claystone and siltstone. Thickness: >67m.Geological Province: Victoria Basin.||||||25-JAN-06
17454|Stubb Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Tijunna Group.   Geological Province: Victoria Basin.||||||
17454|Stubb Formation|28255|3|Fully described|p62, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Basal unit of Auvergne Gp. Deep water deposit - fissile, laminated, dark-grey to red-brown, micaceous shale and coarse sltst becoming coarser upwards. Unconformable over Wondoan Hill Fm; conformable below Jasper Gorge Sst. Max. thick: 115m. See also p68 .||||||
17454|Stubb Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
17454|Stubb Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Interbedded dark grey shale and siltstone; massive quartz sandstone interbeds near top.||||||02-DEC-04
17454|Stubb Formation|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|32660|5|Briefly described|Table 6|||||||||
17454|Stubb Formation|32700|4|Described|Table 1|||Auvergne Group. See p14.||||||05-DEC-06
17454|Stubb Formation|32701|6|Mentioned|p9|||||||||
17454|Stubb Formation|32728|6|Mentioned|p16|||||||||
17454|Stubb Formation|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.||||||02-DEC-04
17454|Stubb Formation|33373|3|Fully described|p9|||On Table 2.||||||
17454|Stubb Formation|33374|6|Mentioned|p8|||Strat. table. See also p12.||||||05-DEC-06
17454|Stubb Formation|33375|6|Mentioned|p11 Tb. 1, p12|Adelaidean|Adelaidean|Fine sandstone and silty sandstone; manganese and iron staining in joints. Max. thickness: ~15m.||||||26-APR-05
17454|Stubb Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group. Fine and silty sandstone.||||||27-APR-05
17454|Stubb Formation|37462|4|Described|Table 4.VI|||||||||
17454|Stubb Formation|45112|3|Fully described|p29|||See p29-30.||||||05-DEC-06
17454|Stubb Formation|45140|6|Mentioned|p13|||Victoria River region.||||||
17454|Stubb Formation|48942|2|Defined|p59|Adelaidean|Adelaidean|||||||
17454|Stubb Formation|48943|3|Fully described|p72|||||||||
17454|Stubb Formation|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Formerly of the Auvergne Group now in Tijunna Group. Interbedded claystone, siltstone, mudstone, sandstone. Conformable on Wondoan Hill Formation; unconforably overlain by Jasper Gorge Sandstone. Max. Thickness: 210m. Geological Province: Victoria Basin.||||||05-DEC-06
17454|Stubb Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Tijunna Group.||Overlies Wondoan Hill Formation. Is unconformably overlain by Jasper Gorge Sandstone of Auvergne Group.||
17454|Stubb Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Tijunna Group.||Overlies Wondoan Hill Formation.|Fine silty sandstone, siltstone.|
17454|Stubb Formation|68733|5|Briefly described|p177 Fig.2, p179-186, p191-192|Cryogenian|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. 1618 +/- 13 Ma. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1618 +/- 13 Ma.|Uppermost unit of the Tijunna Group.||Conformably underlain by the Wondoan Hill Formation. Unconformably overlain by the Jasper Gorge Sandstone.|Dominated by laminated, micaeous shale and silstone, with intercalated quartz sandstone.|06-DEC-17
17454|Stubb Formation|69432|4|Described|p17:2, 12, 15|||Birrindudu Basin. Up to 210m thick. Thick shale may have some potential as petroleum source rock.||Tijunna Group.||Unconformably overlies Banyan Formation.|Lower part is grey shale and red-brown micaceous siltstone; a succession of interbedded micaceous claystone, siltstone, minor mudstone and sandstone.|12-JUL-16
17454|Stubb Formation|69673|6|Mentioned|p48 fig 35|||||Tijunna Group||Overlies Wondoan Hill Formation, unconformably overlain by Auvergne Group||
17454|Stubb Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Tijunna Group.||Shown as overlying Wondoan Hill Formation in map key.|Fine silty sandstone, siltstone.|
17454|Stubb Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Conformably overlies Wondoan Formation. Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).|Siltstone, shale, minor sandstone.|
17454|Stubb Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Overlies Wondoan Hill Formation. Is overlain unconformably by Antrim Plateau Volcanics.|Siltstone, shale, minor sandstone.|
17454|Stubb Formation|70968|2|Defined|vi, p115-117, p120-122, p124, p126-127|Mesoproterozoic|Mesoproterozoic|See also p129, p131-132. Sweet et al. (1974). Originally included in the former Victoria River Group by Traves (1955), and in the former Coolibah Formation by Laing and Allen (1956). Placed in the Auvergne Group by Morgan et al. (1970) and Sweet (1972, 1973), but then excluded by Sweet et al. (1974). Included in Tijunna Group by Beier et al. (2002). Named after Stubb yard, 5km ESE of Victoria Road bridge. The type section is at 52 723532mE 8276218mN (Base) to 52 752241mE 8285144mN in DELAMARE. Variable exposures; crops out extensively from Delamere homestead to the Victoria River. Contains detrital zircons aged c.3100 Ma, derived from the Pilbara or a non-Australian source. Lithology well described and illustrated. Up to 210m thick; 190m in the type section. Represents a regressive sedimentary cycle. Various age determination attempts described. Detrital zircon diagram and discussion.|c.1618 Ma (maximum depositional age).|Tijunna Group.||Overlies Wondoan Hill Formation conformably or Bynoe Formation (Bullita Group) unconformably. Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).|A lower interval has homogeneous green, fissile, laminated micaceous claystone and coarse-grained quartz siltstone that grades upward into white and brown medium-grained quartz sandstone. Local minor thin beds of hematitic sandstone breccia.|24-FEB-17
17454|Stubb Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, siltstone|
17454|Stubb Formation|71302|5|Briefly described|p6,72-74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: 1618+\-13 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Contain small c > 1560-1640 Ma age populations. Also contains small clusters of c. 3100 Ma zircons, interpreted to have been recycled from Pine Creek Orogen sequences (e.g. Crater Formation, Mount Partridge Group; Hollis et al., 2010).||Unit of Tijunna Group.||Overlain by Jasper Gorge Formation. Underlain by Wondoan Hill Formation.||
17454|Stubb Formation|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1618+/-13 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
17454|Stubb Formation|71893|4|Described|p7-p8, p68-p69|||Birrindudu Basin. A maximum depositional age of 1618 +/- 13 Ma was interpreted for this unit in addition to two younger analyses at ca 1485 Ma and 1307 Ma.||Tijunna Group||Conformably overlies the Wondoan Hill Formation.||
17454|Stubb Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Tijunna Group||Underlain by Wondoan Hill Formation.||
17454|Stubb Formation|73083|6|Mentioned|p18|||||||||
17542|Supplejack Downs Sandstone|22446|5|Briefly described|p19|Statherian|Statherian|||||||
17542|Supplejack Downs Sandstone|29809|6|Mentioned|Table 1|||||||||
17542|Supplejack Downs Sandstone|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|29813|6|Mentioned|Table 2|||||||||
17542|Supplejack Downs Sandstone|31361|4|Described|Table 1|||||||||
17542|Supplejack Downs Sandstone|31362|6|Mentioned|Table 1|||||||||
17542|Supplejack Downs Sandstone|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|39887|6|Mentioned|p452|||||||||
17542|Supplejack Downs Sandstone|41883|5|Briefly described|p65|||||||||
17542|Supplejack Downs Sandstone|42643|6|Mentioned|p5|||||||||
17542|Supplejack Downs Sandstone|45140|2|Defined|p12-15, p18, p20-22, p39, p41, p73|Paleoproterozoic|Paleoproterozoic|See also Appx.p7. Blake et al. (1975). Named after Supplejack Downs homestead. The Granites-Tanami Block. The type section is across the S end of a strike ridge 11km E of the homestead, at 19deg 16'50"S, 130deg 02'45"E. At least 1300m thick. Forms a group of sandstone ridges up to 30m high E of the Supplejack Range.|c.1800 Ma.|||Overlies Nanny Goat Creek Beds (Tanami Complex) unconformably and Mount Winnecke Formation ?conformably. Is overlain unconformably by Birrindudu Group and Antrim Plateau Volcanics.|Mainly sublithic arenite and quartz arenite, medium to thin-bedded, commonly close-jointed and cross-bedded, some with layers of shale pellets and rare conglomerate lenses; local shale and siltstone.|
17542|Supplejack Downs Sandstone|45167|5|Briefly described|Fig.27|||||||||
17542|Supplejack Downs Sandstone|46864|6|Mentioned|p37|||||||||
17542|Supplejack Downs Sandstone|48950|2|Defined|p28|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17542|Supplejack Downs Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Sandstone - white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone and shale, minor volcanogenic sandstone; fine- to coarse-grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group||||||07-NOV-08
17542|Supplejack Downs Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Sandstone - white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone, shale, minor volcanogenic sandstone; fine- to coarse-grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Sandstone: white to pale pink, sublithic arenite, quartz arenite, conglomerate, siltstone and shale, minor volcanogenic sandstone; fine to coarse grained, variably sorted.||||||07-NOV-08
17542|Supplejack Downs Sandstone|61861|4|Described|p24, 23, p3 Table 1, p20|Statherian|Statherian|Now included in the Birrindudu Group on basis of lithological and structural similarities with other constituents, particularly Gardiner Sandstone. This study suggests further mapping may rename it as Gardiner or Coomarie Sandstone. Previous possible conformable contact over Mount Winnecke Formation now discounted.||Unit in Birrindudu Group.||Now known to unconformably overlie (or is faulted against) Nanny Goat Volcanics.|Thick-bedded, medium- to coarse-grained quartz arenite and sublithic arenite; contains small clasts of feldspar-quartz ignimbrite just above the base.|03-APR-12
17542|Supplejack Downs Sandstone|63261|5|Briefly described|p12|||Previously assigned to Ware Group, now assigned to Birrindudu Group based on lithological and structural similiarities with Gardiner Sandstone (Birrindudu Group).||||||07-FEB-11
17542|Supplejack Downs Sandstone|64675|6|Mentioned|p9|||See also Supplejack Sandstone.||||Unconformably underlain by the Tanami Complex.||
17542|Supplejack Downs Sandstone|65074|6|Mentioned|p349, p351 fig 4-37|Proterozoic|Proterozoic|Of North/Centre Birrindudu Basin. Early Proterozoic. 1300 m thick.||||Unconformably overlain by Gardiner Sandstone.|Sublithic arenite with minor amounts of shale and siltstone.|
17542|Supplejack Downs Sandstone|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic sandstone;  shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||10-DEC-12
17542|Supplejack Downs Sandstone|65324|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65326|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65338|6|Mentioned|p21.|||Tanami Region. Previously, correlated with Reynolds Range Group (Blake et al. 1979).||||||
17542|Supplejack Downs Sandstone|65349|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17542|Supplejack Downs Sandstone|65352|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65353|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65354|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group. Shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||12-DEC-12
17542|Supplejack Downs Sandstone|65355|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17542|Supplejack Downs Sandstone|65356|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic sandstone; shown as lateral equivalent of Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and interfingering with Gardiner Sandstone||||||12-DEC-12
17542|Supplejack Downs Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent to Gardiner and Coomarie Sandstones and Talbot Well Formation.||Unit in Birrindudu Group.||Unconformably overlies Tanami and Mount Winnecke Groups.||
17542|Supplejack Downs Sandstone|69426|6|Mentioned|p11:5 Fig.11.4|||In Blake et al. (1979).||Birrindudu Group.||||12-JUL-16
17542|Supplejack Downs Sandstone|69432|6|Mentioned|p17:4|||Blake et al. (1975). Subsequently included in the Gardiner Sandstone.||||||12-JUL-16
17542|Supplejack Downs Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, arenite|
17542|Supplejack Downs Sandstone|73083|6|Mentioned|p24|||Intruded by granite of the Tanami Orogen.||||||
17573|Swan Group|13353|6|Mentioned|p398. |||Name replaced by Swan Formation. Includes hydrocarbon source rocks.|||Includes (Lower and Upper) Vulcan Formation.|||
17573|Swan Group|13354|6|Mentioned|p375 Fig.6.|Early Cretaceous|Middle Jurassic|Comprises Lower and Upper Vulcan Formations.||44||||28-OCT-14
17573|Swan Group|22663|5|Briefly described|AC97 1-4 Fig.4|||||||||01-MAR-10
17573|Swan Group|23378|4|Described|p180 Fig.2|Early Cretaceous|Middle Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
17573|Swan Group|41733|6|Mentioned|Fig.3|||||||||
17573|Swan Group|42053|5|Briefly described|Fig.17 P47|||||||||01-MAR-10
17573|Swan Group|42066|5|Briefly described|Fig.3 P199|||||||||
17573|Swan Group|60634|6|Mentioned|p1168 Fig.3. |Early Cretaceous|Late Jurassic||||Includes the Vulcan Formation.|Overlies Troughton Group. Is overlain by Bathurst Island Group.||
17573|Swan Group|61550|6|Mentioned|p495 Fig.2. |Berriasian|Callovian||||Includes the Vulcan and Montara Formations.|Unconformably overlies Plover Formation. Is overlain by Bathurst Island Group.||
17573|Swan Group|66187|5|Briefly described|p413 Fig.2|Berriasian|Oxfordian|Mount Ashmore Dome, Bonaparte Basin. Includes the Upper and Lower Vulcan Formation and Montara Formation.||||||
17573|Swan Group|69297|6|Mentioned|p305|Berriasian|Callovian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin.|||Includes the Montara Formation, the Lower Vulcan Formation and the Upper Vulcan Formation.|Overlies the Troughton Group. Overlain by the Bathurst Island Group.||
17573|Swan Group|69452|5|Briefly described|p36:15|Early Cretaceous|Jurassic|Bonaparte Basin.|||Montara, Vulcan Formations.|||12-JUL-16
17573|Swan Group|70061|6|Mentioned|Regional geology Fig.7. Vulcan: Fig.2|Tithonian|Callovian||||Ashmore Volcanics, Lower and Upper Vulcan Formation, Montara Formation.|||12-JUL-16
17573|Swan Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Valanginian|Callovian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Lower and Upper Vulcan, Montara Formations.|Overlies Troughton Group. Is overlain by Bathurst Island Group.||12-JUL-16
17597|Sydney Heads Pass Conglomerate|23529|4|Described|p23|Proterozoic|Proterozoic|Max. thickness: 30m.   Geological Province: Earaheedy Basin.  See also p26 Fig. 20.||||||
17597|Sydney Heads Pass Conglomerate|23530|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
17597|Sydney Heads Pass Conglomerate|37460|3|Fully described|p157|||||||||
17597|Sydney Heads Pass Conglomerate|37707|6|Mentioned|Table I|||||||||
17597|Sydney Heads Pass Conglomerate|40355|4|Described|p8|||||||||
17597|Sydney Heads Pass Conglomerate|50188|6|Mentioned|p18|||Folded and tilted unit of uncertain age.||||||16-JUL-08
17597|Sydney Heads Pass Conglomerate|64772|5|Briefly described|p16|||Outcrops in small area in northern EARAHEEDY. Up to 20m cobble to boulder conglomerate is exposed in a cliff face; contains clasts of of Earaheedy Group rocks. It post-dates deformation of the Earaheedy Group, but its moderate folding and faulting, suggests it is older than unfolded Neoproterozoic rocks to the north on MUDAN (1:100 000; Hocking et al., 2001a).|?Proterozoic|||||25-NOV-13
17624|Table Hill Volcanics|22517|6|Mentioned|P295||Neoproterozoic III|||||||
17624|Table Hill Volcanics|22650|6|Mentioned|p 159|Early Cambrian|Early Cambrian|Province - Officer Basin.||||||
17624|Table Hill Volcanics|22707|4|Described|P14, Table1 P8||Early Cambrian|Supersedes Officer Volcanics, Age of unit is 575+/-40 Ma.||||||12-NOV-08
17624|Table Hill Volcanics|22716|5|Briefly described|table4, p239|Early Cambrian|Neoproterozoic III|||||||
17624|Table Hill Volcanics|22814|5|Briefly described|p245, fig3|Neoproterozoic|Neoproterozoic|||||||
17624|Table Hill Volcanics|22907|6|Mentioned|39|||||||||
17624|Table Hill Volcanics|23282|6|Mentioned|p79|||Interpreted as synonym of Kulyong Volcanics.||||||
17624|Table Hill Volcanics|23328|5|Briefly described|1029|||Ages: 484+/-4 Ma K-Ar, 575+/-40 Rb-Sr.||||||07-SEP-09
17624|Table Hill Volcanics|23557|5|Briefly described|p96 Fig.2|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|23571|4|Described|p3, 7|Ordovician|Ordovician|Geological Province: Officer Basin. Age: 484 +/- 4Ma. Underlying Unit:  Wahlgu Formation (conformable).||||||
17624|Table Hill Volcanics|23760|5|Briefly described|p25|Early Ordovician|Early Ordovician|||||||
17624|Table Hill Volcanics|23858|5|Briefly described|p919|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|23914|6|Mentioned|p158 Fig. 12|||||||||
17624|Table Hill Volcanics|24067|5|Briefly described|p250|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|24161|4|Described|p7, p9 Tb.6, p21|Early Ordovician|Early Ordovician|Age: 484 +/- 4 Ma. Unconformably overlies the McFadden Formation equivalent. Geological Province: Gunbarrel Basin.||||||
17624|Table Hill Volcanics|24390|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Geological Province: Gunbarrel Basin.||||||
17624|Table Hill Volcanics|24578|5|Briefly described|p792|Cambrian|Cambrian|Age: ~510 Ma.||||||
17624|Table Hill Volcanics|30218|6|Mentioned|p404|||Age discussed||||||
17624|Table Hill Volcanics|30386|6|Mentioned|p8|||||||||
17624|Table Hill Volcanics|30388|4|Described|Table 1|||Table 1 P16. Correlated with Kulyong Volcanics. Ordovician?age.||||||
17624|Table Hill Volcanics|30390|4|Described|p198|||See also P199||||||
17624|Table Hill Volcanics|30944|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
17624|Table Hill Volcanics|30947|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
17624|Table Hill Volcanics|31455|6|Mentioned|p12|||||||||
17624|Table Hill Volcanics|31456|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|31457|4|Described|Table 2|||||||||
17624|Table Hill Volcanics|31459|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31460|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31632|4|Described|Table 2|||See also P10||||||
17624|Table Hill Volcanics|31634|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|31635|4|Described|Table 2|||||||||
17624|Table Hill Volcanics|31636|5|Briefly described|p7|||See also Table 2||||||
17624|Table Hill Volcanics|31638|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31639|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31641|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31642|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|31914|3|Fully described|p96|||Same as Kulyong V. & Officer V.?||||||
17624|Table Hill Volcanics|32648|6|Mentioned|p32|||Ord.||||||
17624|Table Hill Volcanics|33478|6|Mentioned|Table 1|||||||||
17624|Table Hill Volcanics|33590|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|33591|5|Briefly described|p8|||||||||
17624|Table Hill Volcanics|33592|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|33595|4|Described|Table 1|||||||||
17624|Table Hill Volcanics|33625|6|Mentioned|p185|||P197||||||
17624|Table Hill Volcanics|34417|4|Described|p97|||Petrography P99. See also P101||||||
17624|Table Hill Volcanics|35123|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
17624|Table Hill Volcanics|35308|6|Mentioned|Table 1|||||||||
17624|Table Hill Volcanics|36096|6|Mentioned|Fig.3|||||||||
17624|Table Hill Volcanics|36257|6|Mentioned|Table 2.1|||||||||
17624|Table Hill Volcanics|36701|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17624|Table Hill Volcanics|36888|6|Mentioned|p216|||||||||
17624|Table Hill Volcanics|36889|6|Mentioned|p219|||||||||
17624|Table Hill Volcanics|36890|4|Described|p404|||||||||
17624|Table Hill Volcanics|38329|6|Mentioned|Fig.1|||||||||
17624|Table Hill Volcanics|38898|6|Mentioned|p84|||||||||
17624|Table Hill Volcanics|43442|6|Mentioned|p16,21||Cambrian|Previously in Officer Basin||||||
17624|Table Hill Volcanics|43560|6|Mentioned|fig.1,p227|||||||||
17624|Table Hill Volcanics|43561|6|Mentioned|p1443|||||||||
17624|Table Hill Volcanics|43756|6|Mentioned|p542|||Rb-Sr age: 563+/-40 Ma||||||
17624|Table Hill Volcanics|44111|6|Mentioned|p.58, Fig. 2|||in Officer Basin, presented at "Table Hill" only in Fig. 2.||||||
17624|Table Hill Volcanics|44133|4|Described|p39|Middle Cambrian||More than 100m thick. Geological Province: Officer Basin. Age: ~570Ma (poorly constrained, Compston, 1974; Jackson and van de Graaff, 1981).||||||
17624|Table Hill Volcanics|44354|5|Briefly described|Map Legend||Early Cambrian|||||||
17624|Table Hill Volcanics|45104|6|Mentioned|p25|||||||||
17624|Table Hill Volcanics|45149|2|Defined|p34|Neoproterozoic|Neoproterozoic|See also p3 and table 1.||||||22-FEB-17
17624|Table Hill Volcanics|46975|6|Mentioned|p85|||||||||
17624|Table Hill Volcanics|49792|5|Briefly described|Fig.5|||Age 575 +- 40 Ma||||||
17624|Table Hill Volcanics|50085|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Age: ~500Ma.  Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|50205|5|Briefly described|p59 Fig.1,|Ordovician|Ordovician|Of Gunbarrel Basin.|490-480 Ma|||||
17624|Table Hill Volcanics|50327|6|Mentioned|p309|||Basaltic volcanics in the interior of the Australia cration.||||||07-FEB-11
17624|Table Hill Volcanics|50621|5|Briefly described|p167|||Geological Province: Officer Basin.||||||
17624|Table Hill Volcanics|61023|5|Briefly described|p15 Fig. 8|Early Ordovician|Early Ordovician|Geological Province: Gunbarrel Basin.||||||11-APR-08
17624|Table Hill Volcanics|61272|5|Briefly described|p120, p123|Ordovician|Ordovician|Age: 484 +/- 4 Ma (K-Ar). Unconformably overlies the ?McFadden Formation. Overlain by the Lennis and Wanna Formations. See also p123 Fig.4||||||
17624|Table Hill Volcanics|61716|6|Mentioned|p650|Cambrian|Cambrian|Age: 500+/-7Ma (K-Ar, Veevers 2000).||||||
17624|Table Hill Volcanics|61732|5|Briefly described|p4 Fig. 3, p84|Early Ordovician|Cambrian|Basalts. Unconformable on Wahlgu Formation.  Age: 484+/-4Ma (Stevens and Apak 1999). Max. thickness: >483m. Geological Province: eastern Officer Basin.|Age: 484+/-4Ma (Stevens and Apak 1999).|||||07-FEB-11
17624|Table Hill Volcanics|62234|5|Briefly described|p130|Early Ordovician|Late Cambrian|Minimum crystallisation age yielded by plagioclase from evolved dolerite (diabase) lithology: 500.1+/-7Ma (K-Ar). Samples from Nyaninya sill: thin sections found to contain rare zirconolite grains intergrown with matrix feldspar, quartz and chlorite.||||||05-FEB-07
17624|Table Hill Volcanics|62453|4|Described|p5 Fig. 3, 19, 22, 70|Late Cambrian|Middle Cambrian|Geological Province: Officer Basin. Underlies: Lennis Sandstone. Overlies: Lungkarta Formation.||||||
17624|Table Hill Volcanics|62557|5|Briefly described|p461,462,463|Late Cambrian|Middle Cambrian|K/Ar age 500+/-14 Ma (Veevers,2000). Composition likely to be affected by alteration.||||||14-SEP-09
17624|Table Hill Volcanics|62987|5|Briefly described|p30|Middle Cambrian|Middle Cambrian|Geological Province: Gunbarrel Basin.||||||25-NOV-13
17624|Table Hill Volcanics|63022|5|Briefly described|p1013|Silurian?|Middle Cambrian|Coeval with Antrim Plateau Volcanics. Age: 484+/-8Ma (age of alteration not crystallisation). Geological province: Officer Basin.|484+/-8Ma age of alteration, not crystallisation|||||24-NOV-09
17624|Table Hill Volcanics|64068|6|Mentioned|p81|Cambrian|Cambrian|Officer Basin.|500 +/- 7 Ma.|||||05-APR-12
17624|Table Hill Volcanics|64103|6|Mentioned|p398, p400 Fig. 3|Cambrian|Middle Cambrian|Geological Province: Gunbarrel Basin.||||||07-FEB-11
17624|Table Hill Volcanics|64325|5|Briefly described|p82 Fig. 2, p85, p86|Ordovician|Ordovician|Geological Province: Gunbarrel  Basin.||||||26-AUG-08
17624|Table Hill Volcanics|64580|4|Described|map legend||Middle Cambrian|Basalt (in part vesicular and/or amygdaloidal) in multiple flows; interbedded sandstone and siltstone.||||||09-DEC-08
17624|Table Hill Volcanics|64589|4|Described|dated_samples,chemistry files|Cambrian|Neoproterozoic|Basalt.  K-Ar on plagioclase, crystallization age 500.1+/-7.4 Ma. Same material dated by whole-rock and pyroxene Rb/Sr (Compston, 1974) 575+/-40 Ma. Outcrop Nyaninya Sill, Nano-SIMS on zirconolite, crystallization age 504+/-18 Ma. Geochemical analyses.||||||12-NOV-08
17624|Table Hill Volcanics|64772|5|Briefly described|p16|Cambrian|Cambrian|Geological province: Gunbarrel Basin. Significant and widespread magmatic event.||||||25-NOV-13
17624|Table Hill Volcanics|64793|6|Mentioned|p286 Fig.5|Paleozoic|Paleozoic|||||||
17624|Table Hill Volcanics|64970|5|Briefly described|p718, p719, p719 Fig. 2, p720|Ordovician|Cambrian|Underlain by McFadden Formation, angular unconformity. Geological Province: Officer Basin. Also on p721 Fig. 6, 7.||||||
17624|Table Hill Volcanics|65074|6|Mentioned|p358|||Officer Basin.||||Correlated with Antrim Plateau Volcanics.||
17624|Table Hill Volcanics|65102|4|Described|p366, Figure 4-41, p368-373, 370|Early Cambrian|Early Cambrian|Officer Basin. 30-164m. Correlated with Kulyong Volcanics in SA. Basalt flows separated by a thin sandstone unit; subaerial extrusion with intervals of fluvial clastics; unconformable on folded Proterozoic rocks; dated 575+/-40 Ma [Neoproterozoic]; type section east side of Table Hill, 26deg 28min S, 126deg 53min E.||||||
17624|Table Hill Volcanics|65106|5|Briefly described|p130-133|Early Ordovician|Late Cambrian|Samples from Nyaninya sill used in the NanoSIMS 50 ion microprobe. New dating from lead isotopes in zirconolite. The 506 Ma age agrees within error with the previous K-Ar age, demonstrating the capability of the instrument.|500.1 +/-7.4 Ma (K-Ar); 506 Ma.||||Late-stage evolved diorite (diabase).|
17624|Table Hill Volcanics|65313|5|Briefly described|p578|Early Ordovician|Early Ordovician|Dated 484 +/- 4 Ma (Stevens and Apak, 1999).||||Is overlain by Mount Chandler Sandstone.||26-MAR-12
17624|Table Hill Volcanics|65337|6|Mentioned|p95.|||Probably synonymous with Kulyong Volcanics. Possible correlative with Kalkarindji Volcanic Group.||||||
17624|Table Hill Volcanics|65363|6|Mentioned|p5 Fig.4, p7. |Early Ordovician|Cambrian|||||Overlies Lungkarta Formation.||
17624|Table Hill Volcanics|65365|5|Briefly described|p10 Fig. 4||Cambrian|Central Officer Basin||||||
17624|Table Hill Volcanics|65366|5|Briefly described|p23 Fig. 3||Cambrian|Central Officer Basin||||||
17624|Table Hill Volcanics|65410|5|Briefly described|p74.|||Equivalent to the northern Australian Antrim Plateau Volcanics. The age is a recalculation from Compston (1974) but is equivocal; the unit may be as young as Cambrian.|563 +/- 40 Ma.||||Flood basalts.|
17624|Table Hill Volcanics|65416|4|Described|p137, p138 Fig.3, p139 Fig.4, p144, p146|Late Cambrian|Middle Cambrian|Western Officer Basin, SW and NE margins. The basalt flows were previously named the Officer Volcanics in the WA section of the Basin. Part of Sequence Pz1. Eroded in Savory Sub-basin prior to deposition of Paterson Formation. Correlated with Kulyong Volcanics (SA) and Antrim Plateau Volcanics. Extends into SA and is mapped as Kulyong Volcanics near the state border; they constitute a single tholeiitic basalt suite.|575 +/- 40 Ma (Townson 1985).|||Unconformably overlies McFadden Formation and Wirrildar beds. Is overlain unconformably by Lennis Sandstone and Paterson Formation.|Porphyritic and amygdaloidal tholeiitic basalts; basal fluvial sandstones; a sandy, weathered interval between two distinct massive subaerial flows.|
17624|Table Hill Volcanics|65506|5|Briefly described|p986|||Occurs in sedimentary rocks overlying Bangemall Supergroup in the east. Basalt, dolerite. Correlated with ~500 Ma Kalkarindji LIP.||||||23-MAY-17
17624|Table Hill Volcanics|66521|4|Described|p20.|Late Cambrian|Middle Cambrian|Gunbarrel and Officer Basins. Use of this Western Australian name was widened to include the South Australian unit formerly known as Kulyong Formation, because outcrop is more extensive and the unit is thicker and better understood in Western Australia.|K-Ar age of 484 +/- 4 Ma reflects alteration.||||Basalt; sediments.|
17624|Table Hill Volcanics|67195|4|Described|p5, p9 fig5, p10, p19 tbl1, p40,44,45,47|Cambrian|Cambrian|Basal Gunbarrel Basin. Thermal conductivities of 1.57 W/mK and 2.25 W/mK for the basalt and dolerite respectively.  Basal unit of one well in this study. See also App 1, App 2.||||Unconformably overlain by Lennis Sandstone, Wanna Formation, unconformably overlies Lupton Formation, Steptoe Formation|Includes reddish grey basalt and dolerite.|
17624|Table Hill Volcanics|67200|6|Mentioned|app 2 p9, 10||||||||Basalt and dolerite.|
17624|Table Hill Volcanics|67352|6|Mentioned|p31|||Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km.||||||
17624|Table Hill Volcanics|67454|6|Mentioned|p564.|Early Paleozoic|Early Paleozoic|Occupies a higher stratigraphic level than Wahlgu Formation, in Empress 1A drillhole.||||||
17624|Table Hill Volcanics|68902|6|Mentioned|p20, p27|Early Cambrian|Early Cambrian|Base of Gunbarrel Basin. Fed by c.500 Ma dolerite intrusions along N-trending fractures in the Rudall Complex.||||||
17624|Table Hill Volcanics|69003|6|Mentioned|p60|Cambrian|Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|69029|6|Mentioned|p329|Ordovician|Ordovician|Of Officer Basin.||||Overlain unconformably by Lennis Sandstone. Underlain unconformably by Lupton Formation or McFadden Formation or Vines Formation.||
17624|Table Hill Volcanics|69091|5|Briefly described|p30 Fig.3.5, p35, p37, see comments|Late Cambrian|Late Cambrian|Officer Basin. Deformed by a salt diapir and creates distinct gravity peak at -79 mGal as it curves upwards towards surface, and broad gravity low also matches well with extent of this salt diapir at depth. Misspelled as Table Hills Volcanics on p45 and p182. See also p38 Fig.3.7, p41 Fig.3.8, p44-45, p81 Fig.4.17, p105-109, p115 Fig.5.14, p174 Fig.9.5, p176, p177 Fig.9.6, p181-182, p200 Fig.10.2.||||Overlain by Lennis Sandstone and Wanna Formation; overlies with angular unconformity Browne, Hussar and Kanpa Formations, or disconformably over Wahlgu and Lungkarta Formations.|Predominantly basalt flows.|
17624|Table Hill Volcanics|69153|6|Mentioned|500k_geologyp08_lut.csv||Middle Cambrian||||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; interbedded sandstone and siltstone|
17624|Table Hill Volcanics|69445|3|Fully described|p30:1, 5-7, 9, 16-17|Cambrian|Cambrian|Peers (1969). Officer Basin. Synonymous with Kulyong Volcanics. Up to 116m thick. Type section is the east side of Table Hill (26o28'S, 126o53'E) in TALBOT map area. Another age determination is of 500 +/- 14 Ma (K-Ar whole rock; reported in Veevers, 2000).|505 +/- 3 Ma (Ar40/Ar39: Evins et al., 2009).|Kalkarindji Suite.|Boondawari dolerite.|Overlies Trainor Hill Sandstone. Conformably overlies Wahlgu and Lungkarta Formations. Is overlain by Paterson, Lennis and Wanna Formations, Mount Chandler Sandstone.|Coeval basaltic and intrusive rocks.|12-JUL-16
17624|Table Hill Volcanics|70137|5|Briefly described|Map legend.|Cambrian|Cambrian|Officer Basin.|||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone.|
17624|Table Hill Volcanics|70315|6|Mentioned|p23|||Considered part of the Kalkarindji province through geochemical, geochronological and stratigraphic correlation.||||||
17624|Table Hill Volcanics|70634|4|Described|100k_geologyp_lut,csv|Cambrian|Cambrian||508 Ma (Isotopic)||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70793|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Officer Basin (Phase 2). Of Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|508+\-10 Ma; 505+\-3 Ma||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70802|4|Described|250k_pre_mesozoic_interpgeop_lut.csv|Cambrian|Cambrian|Of Officer Basin (Phase 2); Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma).|508+\-10 Ma; 505+\-3 Ma||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|70839|6|Mentioned|p343|||Of East Officer Basin.||||Underlain by Trainor Hill Sandstone and Apamurra Formation.||
17624|Table Hill Volcanics|71146|5|Briefly described|p6, p9, p18, p21-p22|Cambrian|Cambrian|Officer Basin, Kalkarindji Large Igneous Province.|506 +/- 6 Ma|||Unconformably overlain by the Lennis Sandstone and Mount Chandler Sandstone. Overlies the Marla Group.|Volcanics.|
17624|Table Hill Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite, andesite, basalt|
17624|Table Hill Volcanics|71268|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Officer Basin (Phase 2). Of Kalkarindji Large Igneous Province. Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Alice Springs Orogeny (450-295 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 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.|508+\-10 Ma; 505+\-3 Ma||||Basalt in multiple flows; in part vesicular or amygdaloidal; minor interbedded sandstone and siltstone|
17624|Table Hill Volcanics|71800|6|Mentioned|p26 fig 3|Middle Cambrian|Early Cambrian|Officer Basin.||||||
17624|Table Hill Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cambrian|Officer Basin (Phase 2).|508 +/-10 Ma max, 505+/-3 Ma min||||Basalt (in part vesicular and/or amygdaloidal) in multiple flows; minor interbedded sandstone and siltstone.|
17624|Table Hill Volcanics|73083|6|Mentioned|p3|Cambrian|Cambrian|[Superseded by or a constituent of the Kalkarindji Suite]. These rocks comprise one of a series of widely separated exposures of Cambrian basalt attributed to the Kalkarindji Continental Flood Basalt Province (Glass et al, 2013). Correlation was based on matching magnetic signatures.|||||Basalt.|
17668|Talbot Well Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
17668|Talbot Well Formation|23314|5|Briefly described|336|||||||||
17668|Talbot Well Formation|24122|5|Briefly described|p4 Fig.3|||Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Birrindudu Group. Overlies Gardiner Sandstone; overlain by Coomarie Sandstone. Geological Province: Birrindudu Basin.||||||25-JAN-06
17668|Talbot Well Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
17668|Talbot Well Formation|29804|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|29805|4|Described|Table 1|||||||||
17668|Talbot Well Formation|29809|5|Briefly described|p418|||||||||
17668|Talbot Well Formation|29811|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
17668|Talbot Well Formation|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|29813|4|Described|Table 2|||||||||
17668|Talbot Well Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17668|Talbot Well Formation|31361|4|Described|Table 1|||||||||
17668|Talbot Well Formation|31362|4|Described|Table 1|||||||||
17668|Talbot Well Formation|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17668|Talbot Well Formation|36551|6|Mentioned|Table 12|||||||||
17668|Talbot Well Formation|38243|6|Mentioned|p354|||||||||
17668|Talbot Well Formation|42504|5|Briefly described|Table 3 P60|||||||||
17668|Talbot Well Formation|44155|6|Mentioned|p252|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||Equivalent to Bungle Bungle Dolomite, Osmond Range area.||
17668|Talbot Well Formation|45140|2|Defined|p13, p39-43, p54, p58, p74, p83|||See also Appx.p17-18. Blake et al. (1975). Birrindudu Basin. The type section is on the W side of Supplejack Range, at 19deg 16'45"S, 129deg 54'00"E in the Tanami sheet area. Up to 300m thick. Forms low mounds partly covered with chert rubble; locally capped by laterite and silcrete. May correlate with Bungle Bungle Dolomite and part of Limbunya Group.|c.1600 Ma.|Birrindudu Group.||Conformably overlies Gardiner Sandstone. Is overlain conformably by Coomarie Sandstone; unconformably by Antrim Plateau Volcanics.|Typically chert, commonly stromatolitic, locally brecciated; also includes sublithic arenite, quartz arenite, and laminated siltstone and shale which are locally interlayered with chert, and cherty arenite and stromatolitic limestone.|
17668|Talbot Well Formation|46788|6|Mentioned|p10|||||||||
17668|Talbot Well Formation|46864|4|Described|p38|||||||||
17668|Talbot Well Formation|48950|2|Defined|p36|Neoproterozoic|Neoproterozoic|||||||
17668|Talbot Well Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group.  Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Stromatolitic chert, cherty arenite, siltstone, mudstone, limestone, quartz arenite, sublithic arenite.||||||07-NOV-08
17668|Talbot Well Formation|60685|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group. Geological Province: Birrindudu Basin.||||||19-MAY-05
17668|Talbot Well Formation|61861|6|Mentioned|p3 Table 1|Paleoproterozoic|Paleoproterozoic|See also Talbot Wells Formation (pp22-24).||Unit in Birrindudu Group.|||Recessive unit characterised by chert, conmmonly stromatolitic indicating it is silicified limestone or dolomite; also sublithic arenite, quartz arenite and laminated siltstone, shale and minor limestone.|04-APR-12
17668|Talbot Well Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Geological Province: Birrindudu Basin. Stromatolitic chert, cherty arenite, minor siltstone, mudstone, limestone, quartz arenite.||||||07-NOV-08
17668|Talbot Well Formation|63261|5|Briefly described|p7, p9 Fig. 5, p17|||Of Birrindudu Group. Thickness: 500m. Geological province: Victoria-Birrindudu Basin. Sedimentary structures, stromatolites and dolostone present. See also p[17.||||||07-FEB-11
17668|Talbot Well Formation|64662|5|Briefly described|p30 Fig. 3|Statherian|Statherian|Of the Birrindudu Group. Geological Province: Tanami region.||||||07-FEB-11
17668|Talbot Well Formation|64675|6|Mentioned|Fig.2|||||||||
17668|Talbot Well Formation|65074|4|Described|p349, p351 fig 4-37, p352-353|Mesoproterozoic|Mesoproterozoic|See also p354 Tb. 4-11, p362. Of North/Centre Birrindudu Basin. 250m thick. Occurs as low mounds capped by chert rubble. Type section details given.||Birrindudu Group||Overlies Gardiner Sandstone (conformably). Overlain by Coomarie Sandstone (conformably).|Chert, arenite, siltstone, shale, limestone.|
17668|Talbot Well Formation|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||02-FEB-10
17668|Talbot Well Formation|65324|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65326|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Birrindudu Group.||Overlies Gardiner Sandstone. Is overlain by Coomarie Sandstone.||
17668|Talbot Well Formation|65349|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
17668|Talbot Well Formation|65352|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65353|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65354|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
17668|Talbot Well Formation|65355|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non-magnetic chert, arenite, siltstone, mudstone and limestone; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|65356|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group; underlies the Coomarie Sandstone, overlies the Gardiner Sandstone||||||
17668|Talbot Well Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Birrindudu Group.||Overlies Gardiner Sandstone. Is overlain by Coomarie Sandstone, and unconformably overlain by Antrim Plateau Volcanics.|Chert, arenite, siltstone, mudstone, limestone.|
17668|Talbot Well Formation|69426|6|Mentioned|p11:5 Fig.11.4|||In Blake et al. (1979).||Birrindudu Group.||||12-JUL-16
17668|Talbot Well Formation|69432|5|Briefly described|p17:2, 4, 13|Paleoproterozoic|Paleoproterozoic|Occurs along Coomarie and Supplejack Ranges and in structural basin between the Gardiner and Supplejack Ranges, Birrindudu Basin. Topographically subdued. 300-500m thick. Probably a silicified limestone or dolostone-dominated unit that was deposited on a carbonate platform.||Birrindudu Group.|||Stromatolitic chert, locally massive or brecciated and poorly bedded; sublithic sandstone, quartz sandstone, laminated siltstone, shale and minor limestone.|12-JUL-16
17668|Talbot Well Formation|69673|6|Mentioned|p48 fig 35|||||Birrindudu Group||Overlain by Coomarie Sandstone, overlies Gardiner Sandstone||
17668|Talbot Well Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.||Overlies Gardiner Sandstone.|Stromatolitic chert; minor siltstone, mudstone, limestone, quartz sandstone, sublithic quartz sandstone.|
17668|Talbot Well Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.|||Stromatolitic chert, cherty sandstone, minor siltstone, mudstone, limestone, quartz sandstone, sublithic sandstone.|
17668|Talbot Well Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Birrindudu Group.|||Shallow marine stromatolitic chert, thinly bedded sublithic sandstone, laminated siltstone, shale and limestone|
17668|Talbot Well Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Birrindudu Group.||||
17668|Talbot Well Formation|71349|5|Briefly described|p725|||||Birrindudu Group.|||Fine-grained and calcareous.|
17680|Talga Talga Subgroup|22672|6|Mentioned|P268||Archean|Age of unit is 3517+/-80 Ma||||||07-NOV-08
17680|Talga Talga Subgroup|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3520-3400Ma||||||07-NOV-08
17680|Talga Talga Subgroup|22717|6|Mentioned|Fig3 P18||Archean|||||||07-NOV-08
17680|Talga Talga Subgroup|23206|6|Mentioned|Fig.1|||of Warrawoona Fm.||||||
17680|Talga Talga Subgroup|23255|5|Briefly described|p46 Fig.2|||Of Warrawoona Group.||||||21-AUG-07
17680|Talga Talga Subgroup|23388|6|Mentioned|p14 Table 1|||||||||
17680|Talga Talga Subgroup|23416|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group, Pilbara Craton||||||07-NOV-08
17680|Talga Talga Subgroup|23755|5|Briefly described|p17 Table 1|Archean|Archean|Of Warrawoona Group.||||||07-NOV-08
17680|Talga Talga Subgroup|23783|5|Briefly described|p7 Fig.2|||Parent: Warrawoona Group.||||||22-OCT-08
17680|Talga Talga Subgroup|23807|5|Briefly described|p110|||Geological Province: Pilbara Craton.||||||
17680|Talga Talga Subgroup|23895|5|Briefly described|p885 Fig.2, p904|||Overlain by Salgash Subgroup.  Geological Province: Pilbara Craton.||||||07-MAR-05
17680|Talga Talga Subgroup|23936|5|Briefly described|Tb.3|Archean|Archean|Age: 3405 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|24025|4|Described|p9 Tb. 1|Archean|Archean|Includes the Duffer, Dresser and McPhee Formations, and Mount Ada and North Star Basalts. Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|24182|4|Described|p92|||Of the Warrawoona Group. Age: 3490 Ma.  Tholeiitic basalt and komatiite successions. Geological Province: Pilbara Craton.||||||
17680|Talga Talga Subgroup|24184|4|Described|p699, p707 Fig.8|Archean|Archean|Of the Warrawoona Group. Overlain by Salgash Subgroup. Geological Province: Pilbara Craton. Age: ca. 3490-3454Ma. Now includes the former Duffer Formation (Hickman 1990)||||||07-NOV-08
17680|Talga Talga Subgroup|24185|5|Briefly described|p741 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|24194|5|Briefly described|p905|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|24590|5|Briefly described|p29, p30 Fig. 1.3|Archean|Archean|Of the Warrawoona Group. Includes the North Star Basalt. Overlain by Duffer Formation and Salgash Subgroup. Age: ca.3.51Ga (40Ar-39Ar). Thickness: .4.1km.||||||07-FEB-11
17680|Talga Talga Subgroup|31309|6|Mentioned|Table 8|||refs Lipple 1975||||||
17680|Talga Talga Subgroup|31853|2|Defined|p60|Archean|Archean|||||||07-NOV-08
17680|Talga Talga Subgroup|35142|6|Mentioned|p421|||||||||
17680|Talga Talga Subgroup|35531|6|Mentioned|Fig.1|||Composite lithostratigraphic section||||||
17680|Talga Talga Subgroup|37899|6|Mentioned|Fig.2|||||||||
17680|Talga Talga Subgroup|38498|5|Briefly described|Table 1|||||||||
17680|Talga Talga Subgroup|38542|6|Mentioned|p361|||||||||
17680|Talga Talga Subgroup|38544|6|Mentioned|p296|||||||||
17680|Talga Talga Subgroup|38624|6|Mentioned|Fig.2|||||||||
17680|Talga Talga Subgroup|39426|6|Mentioned|Fig.3|||||||||
17680|Talga Talga Subgroup|39444|6|Mentioned|Table 1|||||||||
17680|Talga Talga Subgroup|39580|4|Described|p288|||||||||
17680|Talga Talga Subgroup|39672|6|Mentioned|p240|||||||||
17680|Talga Talga Subgroup|39697|6|Mentioned|p28|||||||||
17680|Talga Talga Subgroup|40596|6|Mentioned|Fig.1|||||||||
17680|Talga Talga Subgroup|41252|6|Mentioned|Table 1|||||||||
17680|Talga Talga Subgroup|41678|6|Mentioned|p30|||||||||
17680|Talga Talga Subgroup|41982|6|Mentioned|Table 1 P1780|||||||||
17680|Talga Talga Subgroup|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
17680|Talga Talga Subgroup|43595|5|Briefly described|p213|||||||||
17680|Talga Talga Subgroup|43689|6|Mentioned|Fig3p166|||||||||
17680|Talga Talga Subgroup|43698|6|Mentioned|p3|||||||||
17680|Talga Talga Subgroup|43769|6|Mentioned|p857|||||||||
17680|Talga Talga Subgroup|44150|5|Briefly described|p129 Tb.2-15, p137-138|||Defined by Lipple (1975). Only 15% is ultramafic.||Warrawoona Group|North Star, Mount Ada Basalts; McPhee Formation.|||
17680|Talga Talga Subgroup|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Warrawoona Group.  Includes the Mount Ada Basalt.||||||07-NOV-08
17680|Talga Talga Subgroup|46319|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Warrawoona Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|50381|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|50423|5|Briefly described|p216||Archean|3490-3470 Ma. Of lower Warrawoona Group.||||||07-NOV-08
17680|Talga Talga Subgroup|50427|4|Described|p182|Archean|Archean|Age: 3490-3460 Ma. Meta basalts. Overlies Coonterunah Group, overlain by Salgash Subgroup and unconformably by Kelley Subgroup. Of Warrawoona Group.||||||07-NOV-08
17680|Talga Talga Subgroup|50544|5|Briefly described|p9, p18|Archean|Archean|Of the Warrawoona Group.||||||07-NOV-08
17680|Talga Talga Subgroup|50555|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group.  Includes the Duffer Formation and Mount Ada Basalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|60112|5|Briefly described|p107 Fig.1. ||||||||Thin volcaniclastic chert.|
17680|Talga Talga Subgroup|60429|5|Briefly described|p7|Archean|Archean|See also p8 Fig. 4.||||||07-FEB-11
17680|Talga Talga Subgroup|61253|5|Briefly described|p51, p52 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Subgroup). Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Warrawoona Group. Includes the McPhee Formation and Mount Ada Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|63420|5|Briefly described|Map legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup).  Includes North Star Basalt and McPhee Formation.  Ages: c.3490Ma and 3477Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
17680|Talga Talga Subgroup|63441|4|Described|p4 Tb. 1, p19|Archean|Archean|Of Warrawoona Gp (Pilbara Supergp). Now comprises North Star Basalt and McPhee Fm. Former components Mount Ada Basalt+Duffer Fm. now included in Coongan Subgroup.Overlain by Coongan Subgp. Age:3490-3477Ma. Max. thickness:3500m. Geol.prov: Pilbara Cr.||||||07-FEB-11
17680|Talga Talga Subgroup|63538|4|Described|p3 Fig. 2, p5, p6 Fig. 3|Archean|Archean|Of Warrawoona Group. Includes McPhee Formation and North Star Basalt. Age: 3490-3477 Ma. Overlain by Coongan Subgroup, underlain by Coonterunah Subgroup. Geological Province: Pilbara Craton.||||||19-APR-13
17680|Talga Talga Subgroup|64328|5|Briefly described|p56 Tb. 1|||Includes Double Bar and Dresser Formations, North Star Basalt, McPhee Formation, Mount Ada Basalt and Duffer Formation.||||||07-FEB-11
17680|Talga Talga Subgroup|64405|5|Briefly described|p2 Fig. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological province: East Pilbara Terrane.||||||07-FEB-11
17680|Talga Talga Subgroup|64580|6|Mentioned|map legend|||||||||
17680|Talga Talga Subgroup|64621|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Includes McPhee Formation and North Star Basalt. Lithological details included.||||||07-NOV-08
17680|Talga Talga Subgroup|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
17680|Talga Talga Subgroup|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Warrawoona Group. Includes Mount Ada Basalt and Duffer Formation. Consists of metamorphosed mafic and felsic volcanics and sedimentary rocks. Geological Province: Pilbara Craton.||||||07-FEB-11
17680|Talga Talga Subgroup|64936|5|Briefly described|map legend|Archean|Archean|Of Warrawoona Group. Includes Duffer Formation, Mount Ada Basalt, McPhee Formation and North Start Basalt. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
17680|Talga Talga Subgroup|65008|5|Briefly described|p8, p9, p41|||East Pilbara Granite-Greenstone Terrane.||Of the Warrawoona Group|Includes Duffer Formation, Mount Ada Basalt.|||
17680|Talga Talga Subgroup|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Warrawoona Group.|Includes Duffer Formation and Mount Ada Basalt.|||
17680|Talga Talga Subgroup|65827|6|Mentioned|p6 Tb.1|Paleoarchean|Paleoarchean|Of Warrawoona Group; formerly included Duffer Formation and Mount Ada Basalt.||||||21-JAN-22
17680|Talga Talga Subgroup|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Warrawoona Group. Consists of North Star Basalt and McPhee Formation.||||||
17680|Talga Talga Subgroup|66217|4|Described|p5, p6 Table 1, p8, p14, pp15-17. |Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Type area is in the Talga Talga Anticline of the Marble Bar greenstone belt; c.2100 m thick. Hickman (1983) defined the Subgroup as consisting of North Star Basalt, McPhee Formation, and Mount Ada Basalt. Van Kranendonk et al. (2006a) assigned the Mount Ada Basalt to the overlying Coongan Subgroup, but included the Duffer Formation in this unit in this (2010) redefinition of the Warrawoona Group.|3490-3477 Ma.|Unit in Warrawoona Group.|Includes North Star Basalt; Dresser and McPhee Formations.|Overlies Coonterunah Subgroup.  Is intruded by Apex Basalt feeder dykes. Is overlain conformably by Coongan Subgroup; unconformably by Strelley Pool Formation and Gorge Creek Group.||
17680|Talga Talga Subgroup|66664|6|Mentioned|p3.  |||East Pilbara Terrane||Unit in Warrawoona Group.|Includes Dresser Formation.|Overlies Coonterunah Subgroup. Is overlain by Coongan Subgroup.||
17680|Talga Talga Subgroup|66745|5|Briefly described|p57.|Paleoarchean|Paleoarchean|||Unit in Warrawoona Group.|Includes Dresser and McPhee Formations and North Star Basalt.|Is disconformably overlain by Coongan Subgroup.||
17680|Talga Talga Subgroup|67197|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|North Star Basalt; McPhee, Dresser Formations.|||
17680|Talga Talga Subgroup|67201|5|Briefly described|p7 Fig.4|||In northern Pilbara Craton, East Pilbara Terrane.||Warrawoona Group|McPhee Formation and Dresser Formation, North Star Basalt|||
17680|Talga Talga Subgroup|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Warrawoona Group.|North Star Basalt; McPhee, Dresser Formations.|Is overlain by Coongan Subgroup.||
17680|Talga Talga Subgroup|67270|5|Briefly described|p3-4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|North Star Basalt; McPhee and Dresser Formations.|Overlies Coonterunah Subgroup. Is overlain by Dresser Formation.||
17680|Talga Talga Subgroup|68035|4|Described|p288 Fig 4|Paleoarchean||Pilbara Supergroup, East Pilbara Terrane.||Of Warrawoona Group. |Includes North Star Basalt, McPhee Formation, Dresser Formation|Disconformably overlain by Coongan Subgroup.|Basalt, lesser chert, komatiitic basalt, minor felsic volcanics, siliciclastic rocks, komatiite.|
17680|Talga Talga Subgroup|68280|6|Mentioned|p4|||||Warrawoona Group|Includes North Star Basalt, McPhee Formation, Dresser Formation||Basalt.|
17680|Talga Talga Subgroup|68283|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes McPhee Formation, North Star Basalt.|||23-SEP-13
17680|Talga Talga Subgroup|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Warrawoona Group.|McPhee, Dresser Formations; North Star Basalt.|Is overlain by Coongan Subgroup.||
17680|Talga Talga Subgroup|69012|5|Briefly described|Map Legend|Archean|Archean||>3490-c.3477 Ma|Of the Warrawoona Group.|Includes the McPhee Formation and the North Star Basalt.|||28-APR-14
17680|Talga Talga Subgroup|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Warrawoona Group.|Includes the Dresser Formation, McPhee Formation, and North Star Basalt.|||
17680|Talga Talga Subgroup|69167|6|Mentioned|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|Includes Mcphee Formation, Dresser Formation, North Star Basalt, Mount Ada Basalt|||
17680|Talga Talga Subgroup|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of Warrawoona Group.|Includes Dresser Formation.|||
17680|Talga Talga Subgroup|69301|4|Described|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||Warrawoona Group|McPhee Formation, Dresser Formation, North Star Basalt|||
17680|Talga Talga Subgroup|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_geologyp08_lut.csv.||Unit of Warrawoona Group.|Includes Dresser Formation, McPhee Formation, North Star Basalt.|||
17680|Talga Talga Subgroup|70022|6|Mentioned|p115|||East Pilbara Terrane.||Warrawoona Group.|North Star Basalt; McPhee, Dresser Formations.|||
17680|Talga Talga Subgroup|70729|6|Mentioned|p164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Includes Dresser Formation.|||
17680|Talga Talga Subgroup|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||Warrawoona Group.|Dresser Formation.|||
17680|Talga Talga Subgroup|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Includes Mc Phee and Dresser formations, and North Star Basalt.|Overlain by Mount Coongan Subgroup/Ada Basalt. Underlain by Coonterunah Subgroup/Double Bar Formation.||
17680|Talga Talga Subgroup|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||chert, mafic and ultramafic schist, amphibolite|
17680|Talga Talga Subgroup|71487|5|Briefly described|p128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.|Incldues Dresser Formation.|Overlain by Coongan Subgroup. Underlain by Coonterunah Subgroup.||
17680|Talga Talga Subgroup|72034|6|Mentioned|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes McPhee Formation, Dresser Formation, North Star Basalt.|||
17680|Talga Talga Subgroup|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawonna Group.|Includes McPhee and Dresser formations and North Star Basalt.|Overlain by Coongan Subgroup. Underlain by Coonterunah Subgroup.||
17680|Talga Talga Subgroup|72668|5|Briefly described|p4, p19|||East Pilbara Terrane.|c. 3490-3477 Ma|Warrawoona Group|Includes the McPhee Basalt, Dresser Basalt and the North Star Basalt.|Overlain by the Coongan Subgroup. Overlies the Coonterunah Subgroup.||
17680|Talga Talga Subgroup|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Warrawoona Group.|North Star Basalt; McPhee, Dresser Formations.|Overlies Coonterunah Subgroup. Is overlain by Coongan Subgroup.||
17696|Talisman Member|42598|3|Fully described|p90|Berriasian||Reserved as Talisman Sandstone.||||||
17696|Talisman Member|60379|6|Mentioned|p126 fig 3|Early Cretaceous|Early Cretaceous|Dampier sub-basin, Carnarvon Basin||Of Forestier Claystone||||
17719|Tamala Limestone|9173|5|Briefly described|Map legend.|Quaternary|Quaternary|Mentioned as a possible equivalent to a mapped unit of calcareous shelly sandstone and grit in coastal dunes, sheets and foreshore reefs.||||||
17719|Tamala Limestone|11797|5|Briefly described|map legend|Pleistocene|Pleistocene|Shark Bay Area. Includes unnamed sub-unit of mobile unvegetated sand sheets and dunes.|||||Unconsolidated to strongly lithified, locally quartzose calcarentie; large-scale eolian cross-bedding.|
17719|Tamala Limestone|12729|6|Mentioned|Fig. 6|Quaternary|Quaternary||||||Limestone.|
17719|Tamala Limestone|12759|4|Described|p49; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined Playford et al. (1975,1976). Type section: Womerangee Hill. Described by Nidagal and Davidson (1991). Max thickness 110 m. Has solution cavities; part of a major aquifer.||||Unconformably overlies Leederville, Osborne, Lancelin Formations, or Bassendean Sand; unconformably underlies Becher or Safety Bay Sands.|Creamy white to yellow, or light grey, calcareous eolianite, with varying proportions of quartz sand, shell fragments and minor clayey lenses; local basal glauconite and phosphatic nodules.|12-MAY-14
17719|Tamala Limestone|14228|6|Mentioned|p5 fig 2|Recent|Pliocene|||||||
17719|Tamala Limestone|22535|6|Mentioned|p494|||||||||
17719|Tamala Limestone|22552|5|Briefly described|p 31, 33, 42|Pleistocene||||||||
17719|Tamala Limestone|22717|5|Briefly described|P14||Quaternary|Formerly the Coastal Limestone||||||
17719|Tamala Limestone|22731|6|Mentioned|p545|||||||||
17719|Tamala Limestone|22742|5|Briefly described|p116, p118 Fig. 3|Pleistocene|Pleistocene|Unconformably overlies Leederville Formation. Unconformably overlain by Leschenault Formation||||||05-NOV-14
17719|Tamala Limestone|22814|6|Mentioned|p258|Quaternary|Quaternary|||||||
17719|Tamala Limestone|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
17719|Tamala Limestone|23279|6|Mentioned|p7,Fig39p43|||||||||
17719|Tamala Limestone|23572|5|Briefly described|p8 Fig. 6|Pliocene|Pliocene|Geological Province: Carnarvon Basin.||||||
17719|Tamala Limestone|23578|5|Briefly described|p8|||||||||
17719|Tamala Limestone|23579|5|Briefly described|Map Legend|||||||||
17719|Tamala Limestone|23726|5|Briefly described|p15|||Underlain by Peron Sandstone. Geological Province: Carnarvon Basin. Max. thickness: >300 m.||||||06-AUG-07
17719|Tamala Limestone|23753|6|Mentioned|Map legend notations|Quaternary|Quaternary|||||||
17719|Tamala Limestone|23754|6|Mentioned|Map Legend|||||||||
17719|Tamala Limestone|23768|5|Briefly described|p30 Fig.6|Pleistocene|Pleistocene|Geological Province: Perth Basin.  See also p136.||||||29-MAR-05
17719|Tamala Limestone|23788|5|Briefly described|p36|Quaternary|Quaternary|||||||
17719|Tamala Limestone|23935|5|Briefly described|p11 Fig.7|Pliocene|Pliocene|Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
17719|Tamala Limestone|24160|6|Mentioned|p94|Quaternary|Quaternary|Perth Basin.||||||
17719|Tamala Limestone|24165|6|Mentioned|p51, p74|||Forms cliffs behind the beach in Stokes Inlet area. Quarried for aggregate for road-building.||||||
17719|Tamala Limestone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Coarse-medium-grained calcarenite, skeletal fragments, quartz sand; well bedded, large-scale cross bedding. Contains soil horizons and calc. structures. Overlain by Safety Bay Sand. Geol. Prov: Perth Basin.||||||24-NOV-09
17719|Tamala Limestone|24464|4|Described|p331|||||||||
17719|Tamala Limestone|24542|5|Briefly described|p5|Holocene|Pleistocene|Unconformably overlies Leeuwin Complex. Eolian calcarenite.||||||
17719|Tamala Limestone|24595|5|Briefly described|p587 Fig. 2|Quaternary|Quaternary|See also p589.||||||
17719|Tamala Limestone|29693|6|Mentioned|p35|||||||||
17719|Tamala Limestone|32645|6|Mentioned|Map legend|early Holocene|Pleistocene|Pleistocene to Early Holocene.||||||
17719|Tamala Limestone|34734|6|Mentioned|p109|||||||||
17719|Tamala Limestone|35093|3|Fully described|p13|||||||||
17719|Tamala Limestone|36199|6|Mentioned|p1|||||||||
17719|Tamala Limestone|36257|6|Mentioned|Table 2.1|||||||||
17719|Tamala Limestone|36293|3|Fully described|p210|||Type section designated.||||||24-MAY-21
17719|Tamala Limestone|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|37308|5|Briefly described|Fig.3|||||||||
17719|Tamala Limestone|37577|6|Mentioned|p74|||See also P85.||||||
17719|Tamala Limestone|38142|6|Mentioned|p322|||||||||
17719|Tamala Limestone|38485|4|Described|p18|||||||||
17719|Tamala Limestone|38777|4|Described|p30|||||||||
17719|Tamala Limestone|38954|6|Mentioned|Table 1|||||||||
17719|Tamala Limestone|38997|4|Described|p5|||||||||
17719|Tamala Limestone|38998|4|Described|p25|||See also p5.||||||06-AUG-07
17719|Tamala Limestone|39155|5|Briefly described|p18|||Hydrogeology||||||
17719|Tamala Limestone|39554|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
17719|Tamala Limestone|39697|6|Mentioned|p140|||||||||
17719|Tamala Limestone|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|39915|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|40110|6|Mentioned|p228|||||||||
17719|Tamala Limestone|40304|5|Briefly described|p42|||See also p38.||||||06-AUG-07
17719|Tamala Limestone|40340|4|Described|p15|||||||||
17719|Tamala Limestone|40341|6|Mentioned|Map legend|early Holocene|Pleistocene|Pleistocene - Early Holocene||||||
17719|Tamala Limestone|40348|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|40349|6|Mentioned|Table 2|||||||||
17719|Tamala Limestone|40359|5|Briefly described|p28|||||||||
17719|Tamala Limestone|40360|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|40367|2|Defined|p73-74|Pleistocene|Pleistocene|Formerly "Coastal Limestone" (Playford et al 1976). Unconformable on Australind Fm; unconform. overlain by Eaton Sand. Max. thick: ~6m. Composed of four main sediment/limestone types, chiefly skeletal grainstones and packstone (details given in article).||||||07-AUG-07
17719|Tamala Limestone|40400|6|Mentioned|p109|||Superseded "Coastal Limestone" of Passmore (1970). Overlain by Bridport Calcilutite - with sharp, unconformable contact. Geological Province: Perth Basin.Calcreted aeolianite limestone.||||||06-AUG-07
17719|Tamala Limestone|40401|6|Mentioned|p121|||||||||
17719|Tamala Limestone|40617|6|Mentioned|p18|||||||||
17719|Tamala Limestone|40731|6|Mentioned|p31|||||||||
17719|Tamala Limestone|40902|6|Mentioned|p55|||||||||
17719|Tamala Limestone|40991|5|Briefly described|p6|||||||||
17719|Tamala Limestone|41200|5|Briefly described|p27|Pleistocene|Pleistocene|Sharp, unconformable contact with Bridport Calcilutite above.||||||06-AUG-07
17719|Tamala Limestone|41251|6|Mentioned|p36|||||||||
17719|Tamala Limestone|41271|4|Described|p196|||Mention p15.||||||06-AUG-07
17719|Tamala Limestone|41341|6|Mentioned|p11|||Formerly Coastal Limestone||||||
17719|Tamala Limestone|41342|4|Described|p7|||||||||
17719|Tamala Limestone|41344|6|Mentioned|p94|||||||||
17719|Tamala Limestone|41346|6|Mentioned|p63|||||||||
17719|Tamala Limestone|41422|6|Mentioned|p163|||||||||
17719|Tamala Limestone|41438|6|Mentioned|Fig.23|||||||||
17719|Tamala Limestone|41502|5|Briefly described|p95|||||||||
17719|Tamala Limestone|41504|6|Mentioned|p71|||||||||
17719|Tamala Limestone|41538|6|Mentioned|p310|||||||||
17719|Tamala Limestone|41544|6|Mentioned|p17|||||||||
17719|Tamala Limestone|41634|4|Described|p41|||||||||
17719|Tamala Limestone|41782|4|Described|p24|||See also Table 2||||||
17719|Tamala Limestone|41783|4|Described|p46|||||||||
17719|Tamala Limestone|41788|5|Briefly described|p109|||||||||
17719|Tamala Limestone|41789|5|Briefly described|p87|||||||||
17719|Tamala Limestone|41831|3|Fully described|p556|||||||||
17719|Tamala Limestone|41912|6|Mentioned|p31|||||||||
17719|Tamala Limestone|41986|4|Described|p41|||||||||
17719|Tamala Limestone|42009|6|Mentioned|p75|||||||||
17719|Tamala Limestone|42116|6|Mentioned|p11|||||||||
17719|Tamala Limestone|42569|5|Briefly described|p81|||||||||
17719|Tamala Limestone|42687|6|Mentioned|map legend|||||||||
17719|Tamala Limestone|42688|6|Mentioned|map legend|||||||||
17719|Tamala Limestone|42715|5|Briefly described|p1014|||||||||
17719|Tamala Limestone|43038|6|Mentioned|p48|||||||||
17719|Tamala Limestone|43062|4|Described|p26,Table 2.p18|||||||||
17719|Tamala Limestone|43096|5|Briefly described|p6|||||||||
17719|Tamala Limestone|43189|5|Briefly described|Map Legend||Pleistocene|||||||
17719|Tamala Limestone|43197|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43212|5|Briefly described|p6||Pleistocene|||||||
17719|Tamala Limestone|43216|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43217|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43231|4|Described|p12||Pleistocene|Diachronous units, Middle to Late Pleistocene||||||
17719|Tamala Limestone|43296|5|Briefly described|Map Legend||Quaternary||0.117 - 0.133 Ma|||||06-DEC-13
17719|Tamala Limestone|43297|4|Described|p1,p17.||Pleistocene|Previously known as 'Coastal Limestone'||||||
17719|Tamala Limestone|43304|5|Briefly described|Map Legend||Pleistocene|||||||
17719|Tamala Limestone|43306|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43308|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43309|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43310|5|Briefly described|Map Legend||Quaternary|||||||
17719|Tamala Limestone|43347|4|Described|10|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|43495|4|Described|3-36|Pleistocene|Pleistocene|||||||
17719|Tamala Limestone|43504|4|Described|1,23||Late Pleistocene|C14 dating: >37 000 years Bp||||||
17719|Tamala Limestone|43796|5|Briefly described|p244|||||||||
17719|Tamala Limestone|44144|4|Described|p501 Tb.4-21, p520-521 Figs.4-165, -166|Pleistocene|Pleistocene|Type Section: Womerangee Hill (Carnarvon Basin) 26o52'S 113o48'E. Over 150m thickness of shoreline and dune sands.||Kwinana Group||Overlies Wadjemup Formation and Rockingham Sand. Overlain by Cooloongup Sand, Safety Bay Sand and (disconformably) Herschell Limestone.|Coarse- to medium-grained calcarenite; minor quartz sand.|
17719|Tamala Limestone|49942|5|Briefly described|p4 Fig.3|Quaternary|Quaternary|Geological Province: Gascoyne Platform.||||||
17719|Tamala Limestone|50022|5|Briefly described|p303|Pleistocene|Pleistocene|Carbonate aeolianite.||||||
17719|Tamala Limestone|60384|6|Mentioned|p243, Fig 2a|Quaternary||Perth and Southern Carnarvon Basins.||||||
17719|Tamala Limestone|61155|5|Briefly described|p6|Holocene|Pleistocene|Carbonate-rich aeolianites. Geological Province: Perth and Carnarvon Basins.||||||
17719|Tamala Limestone|61273|5|Briefly described|p83, p87|Pleistocene|Pleistocene|Calcarenite rock used as dimension stone.||||||
17719|Tamala Limestone|61517|5|Briefly described|p312|Pleistocene|Pleistocene|Contains fossiliferous palaeosols.||||||27-MAY-06
17719|Tamala Limestone|61521|5|Briefly described|p4|Pleistocene|Pleistocene|Cemented aeolinite and shallow marine carbonate sequences; coastal limestone/calcarenite gravel. Geological Province: Rottnest Shelf region. See also p44 Fig.21.||||||26-JUL-06
17719|Tamala Limestone|61811|4|Described|p8, p11, pp17-18, p32, pp48-53, p65.|Pleistocene|Pleistocene|Makes up the sea cliffs north of the Murchison River mouth, and extends up to 20 km inland. Thickness varies from 15 to 300 m. U-series ages from corals in growth positions by Stirling et al.(1998). Hosts The Pinnacles in Nambung National Park. Type section details in Appendix 1.|123.5 +/- 0.5 ka to 121.7 ka .||Includes Cape Burney Sandstone Member and Bootenall Limestone Member.|Overlies Birdrong Sandstone.|Coral reefs of bafflestone and bindstone, mainly of Acropora in a shelly calcarenite-calcirudite matrix; calcareous aeolian deposit.|
17719|Tamala Limestone|62020|6|Mentioned|p179|Pleistocene|Pleistocene|Obsolete name of Playford et al. (1976) for the Coastal Limestone. It was superseded in turn by Kooallup and Tims Thicket Limestones and Myalup Sand (Semeniuk, 1995).||||||
17719|Tamala Limestone|62369|6|Mentioned|p414|||Includes the Minim Cove Member. Geological Province: Perth Basin.||||||
17719|Tamala Limestone|62732|5|Briefly described|p5, p7|||Surrounded by residual sands formed from erosion of the limestone. Composed of medium- to coarse-grained aeolian calcareous sandstone to sandy limestone (calcarenite). Frequently leached at the surface producing a yellow to white quartz sand residue.||||||07-FEB-08
17719|Tamala Limestone|63330|6|Mentioned|p192|||Coastal limestone. Geological Province: Perth Basin/Swan Coastal Plain.||||||31-JAN-08
17719|Tamala Limestone|63454|6|Mentioned|p70|||||||||
17719|Tamala Limestone|63745|5|Briefly described|p62 Fig. 2, p66, p67|Late Pleistocene|Late Pleistocene|See also p60 Fig. 6, p71 Fig. 7.||||||07-FEB-11
17719|Tamala Limestone|63807|4|Described|p10-11|Holocene|Pleistocene|Dune limestone - aeolian calcarenite. Minimum age is Middle Holocene. Thickness: ~115m.||||||31-JAN-08
17719|Tamala Limestone|64580|4|Described|map legend||Quaternary|Of Kwinana Group. Calcarenite and calcareous sandstone; local units of shelly limestone (calcarenite to calcirudite); largely eolian.||||||09-DEC-08
17719|Tamala Limestone|64635|5|Briefly described|p7, p11, p14, p28-29, p32   |Pleistocene|Pleistocene|Caps coastal gorges; forms sea cliffs north of Murchison River mouth. Extends 20 km inland. Hosts the limestone Pinnacles in Nambung National Park.|||||A calcareous aeolian deposit, with a single coral reef facies at Leander Point.|
17719|Tamala Limestone|64769|5|Briefly described|p4, p29, p30 Tb. 4, p32, p34, p61, p73|Pleistocene|Pleistocene|Fine- to coarse-grained, cream to pale brown, eolian calcarenite. Also found on p128 Fig. 130, p129 Fig. 132, p130 Fig. 133, p136, p138 Fig. 141, p139.||||||05-MAY-09
17719|Tamala Limestone|67135|5|Briefly described|p22, p52, pp62-63.|||Extensive unit, long quarried for construction. Rockfalls have been documented on steeper slopes of this unit. Karst landform areas mapped, especially Yanchep-Wanneroo and Leeuwin-Naturaliste regions.||||||
17719|Tamala Limestone|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Peron Sandstone, Bibra Limestone|Planar cross bedded limestone and sandstone.|
17719|Tamala Limestone|68811|5|Briefly described|p70, p71, p73-p75, p90|Pleistocene|Pleistocene|Approximately 115m thick. Forms an aquifer on Rottnest Island. See also p94, p126 tbl 13, p153 app 1, p171 tbl 32, p172 tbl 33, p181.|||||Sandy and variably lithified, medium to coarse-grained sands with shell fragments.|
17719|Tamala Limestone|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
17719|Tamala Limestone|69182|6|Mentioned|Ch2 p3|||Perth Basin.||||||
17719|Tamala Limestone|69558|2|Defined|p3, p65-67, p76, p79-83, 98-106|Middle Pleistocene|Middle Pleistocene|Perth and Carnarvon Basins. A distinctive unit that is well developed on the west side of Edel Land Peninsula. Lithology description is derived from the type section. Outcrops variably on Dirk Hartog, Bernier, Dorre and Koks Islands. Overlain by Holocene sand dunes (unnamed). Forms precipitous cliffs (including the Zuytdorp fault-line scarp cliffs) that may be up to 150m high but are generally between 10-50m high. Originally the 'Coastal Limestone' of Saint-Smith, 1912 and the 'Tamala Eolianite' of Logan (1968) but was renamed the Tamala Limestone by Playford et al (1976b) who also defined a type section as the cliff face below the north side of Womerangee Hill on Tamala Station. At the type section it is at least to 287m thick (as it extends below sea level also). The type section is provided in detail. See also p85, p88 fig 134, p89 fig 136, p90, p95, p98, p99, p101-p106, p113, p137, p252-p254, p260.||||Is equivalent to the Bundera Calcarenite, Peron Sandstone, Bossut Formation and possibly also the Exmouth Sandstone.|Sandy limestone (eolianite) with thin soil and calcrete layers. The top of this unit is marked by a thick layer of calcrete.|24-MAY-21
17719|Tamala Limestone|69788|4|Described|p1023-1037|Pleistocene|Pleistocene|Formerly Tamala Eolianite (Gill, 1968) and Coastal Limestone (Teichert, 1947, 1950; Passmore, 1970). Type locality is at Zuytdorp Cliffs, on Tamala Station in Shark Bay area. Corresponds geologically to the Spearwood Dune System. Karst features are well-developed.|||Includes White Desert, Nambung, Stockyard Gully, Pinnacles Desert and Grey Members.|Is overlain by Cooloongup Sand.|Mainly eolian calcarenite: large-scale, commonly high-angle cross-bedding, high matrix porosity and relatively weak cementation; some marine units, including shell beds. Eolian units separated by paleosols with higher proportions of quartz and clay.|
17719|Tamala Limestone|69840|4|Described|p182-4, p185-190, p193-195, p198|Pleistocene|Pleistocene|See also p200, p186 Fig.3, p188 Fig.5, p196 Fig.13, p197 Fig.14. Synonymous with Spearwood Dune System. Also shown as Tamala Limestone Formation p185. Parallel to the coast, located between Quindalup and Bassendean Dune System. Karst features are present including well developed caves.|c. 0.5 - 0.074 Ma||Includes White Desert Member, Nambung Member, Stockyard Gully Member, Pinnacles Desert Member and Grey Member|Undivided Tamala Limestone shown as underlying all its members. Overlain by Cooloongup Sand, Safety Bay Sand. Underlain by Bassendean Sand, Kockatea Shale.|Aeolian calcarenite, calcretes and paleosols. Quartz sand.|
17719|Tamala Limestone|70097|5|Briefly described|p19 Fig.3, p20 Fig.4|Pleistocene|Pleistocene|Perth Basin. Mandurah Terrace, Bunbury Trough and Dongara Saddle.||||Overlies Yoganup or Yarragadee Formations.|?Limestone.|12-SEP-17
17719|Tamala Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite, beach sediments, coastal sediment, sand, eolian|
17719|Tamala Limestone|71377|5|Briefly described|p7|Quaternary|Neogene|Perth Basin.||||||
17719|Tamala Limestone|71958|5|Briefly described|p35|Late Pleistocene|Middle Pleistocene|Vlaming Sub-basin within the carbonate aeolianite province (the most extensive build up of quaternary carbonate aeoliniate in the world). Exposed in outcrops on the Garden and Rottnest islands. On Rottnest Island it extends to just over 68m below modern sea level (Glenister et al., 1959; Playford, 1988).||||Intercalated with the Rottnest Limestone.||
17719|Tamala Limestone|72034|5|Briefly described|500k_interpgeop16_lut|Late Pleistocene|Middle Pleistocene|Perth Basin; Southern Carnarvon Basin.  Age from biostratigraphy.||Kwinana Group|||Calcarenite and calcareous sandstone; local units of shelly limestone (calcarenite to calcirudite); largely eolian.|
17719|Tamala Limestone|73206|6|Mentioned|p856|||Eolian origin.||||||
17719|Tamala Limestone|73423|4|Described|p1-7|Quaternary|Quaternary|Exposed on the coast of Western Australia. One of the most geographically-extensive deposits of carbonate aeolianite in the world; linear extent of ca 1000 km. Exemplifies syngenetic karstification. New U-Th-Pb ages indicate speleogenesis has occurred for at least the last 200 kyr [see article for details on speleothem dating]. Unit may actually be much older than previous suspected, particularly in the south (e.g., formation onset at 2 Ma?). Lipar and Webb (2014) identified five [informal] members in the Nambung National Park. The unit may be strongly diachronous. There are significant correlations between depositional ages and sea-level highstands.|0.8 - 0 Ma|||Unconformably underlain by Leeuwin Complex.|Carbonate sequence including aeolianites, palaeosols, calcretes, microbialites and shallow marine limestones.|
17719|Tamala Limestone|73424|6|Mentioned|p2|Pleistocene|Pleistocene||||||"Quartzose calcarenite (""beachrock"")."|
17763|Tanami Group|23809|5|Briefly described|p3, p6 Tb. 3|||Overlies the MacFarlane Peak Group with inferred disconformity. Intruded by Repulse Aplite.||||||22-DEC-08
17763|Tanami Group|24197|5|Briefly described|p81|Paleoproterozoic|Paleoproterozoic|Part of the Tanami Complex? (names used interchangeably?). Age: ~2450Ma. Geological province: The Granites-Tanami Block.||||||07-FEB-11
17763|Tanami Group|24442|6|Mentioned|p29|||||||||
17763|Tanami Group|45112|6|Mentioned|p15|||||||||
17763|Tanami Group|50152|5|Briefly described|p71|||Includes; Dead Bullock Formation and Killi Killi Formation.||||||
17763|Tanami Group|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Twigg Formation, Killi Killi Formation, Dead Bullock Formation. Age: ~1880-<1835Ma.||||||07-NOV-08
17763|Tanami Group|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Dead Bullock, Killi Killi and Twigg Formations.||||||07-NOV-08
17763|Tanami Group|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the Dead Bullock, Killi Killi and Twigg Formations. Mainly dolerite; siltstone, sandstone chert; jasperitic chert; sandstone; siltstone.||||||07-NOV-08
17763|Tanami Group|50589|5|Briefly described|p1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Granites-Tanami Block. Age: 2450Ma? (single zircon from granite sill intruding the Group) to 1815Ma. The names Tanami Group and Tanami Complex appear to be used interchangeably.||||||07-NOV-08
17763|Tanami Group|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation. Undifferentiated mafic volcanics and meta-sediment; dolerite; undifferentiated Tanami Group; siltstone, sandstone, chert; jasperlitic chert.||||||07-NOV-08
17763|Tanami Group|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Includes the Killi Killi and Dead Bullock Formations.  Age: 1860-1830Ma.||||||
17763|Tanami Group|61056|5|Briefly described|p777-778|Paleoproterozoic|Paleoproterozoic|Has been used to refer to Tanami Complex . Comprises basal quartzite, pelitic to semi-pelitic schists in the middle, and metamorphosed turbiditic sequence at the top. Overlain by Pargee Sandstone.||||||07-NOV-08
17763|Tanami Group|61246|5|Briefly described|p1, p22|Paleoproterozoic|Paleoproterozoic|Overlain by Ware Group. Age: 1850-1830 Ma. Lateral equivalent of Lander Rock beds.||||||07-NOV-08
17763|Tanami Group|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Killi Killi Formation. Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
17763|Tanami Group|61861|5|Briefly described|p3 Table 1, p4, pp9-14, p23, Map 1|Paleoproterozoic|Paleoproterozoic|This name (of Blake et al 1973) reinstated after use of 'Tanami Complex' for some years. Interpreted as a transgressive passive margin sequence. Hosts gold deposits. Older than Mount Charles Formation.|||Now includes Dead Bullock, Killi Killi and Twigg Formations.|Unconformably overlain by Pargee Sandstone and Mount Charles Formation.||04-APR-12
17763|Tanami Group|62377|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Metasediments. Overlain by Ware Group.||||||07-NOV-08
17763|Tanami Group|62580|5|Briefly described|p9, p21, p54|Paleoproterozoic|Paleoproterozoic|Thick clastic sediments. Overlies MacFarlane Peak Group.||||||07-FEB-11
17763|Tanami Group|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier.||||||07-NOV-08
17763|Tanami Group|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province.||||||07-NOV-08
17763|Tanami Group|62636|6|Mentioned|Map Legend|||Solid Geology legend.|||Killi Killi Formation.|||15-APR-11
17763|Tanami Group|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region - Aileron Province.||||||23-DEC-09
17763|Tanami Group|63261|4|Described|p9 Fig. 5, p10-12|Paleoproterozoic|Paleoproterozoic|Of Blake et al (1973). Also known as Tanami Complex (Blake et al 1975). Contains basal Dead Bullock Fm+overlying Killi Killi Fm. Age:1880-1830Ma. Metasedimentary succession. Geological province: Tanami Region.|Age:1880-1830Ma.||basal Dead Bullock Fm+overlying Killi Killi Fm|||07-FEB-11
17763|Tanami Group|63866|6|Mentioned|p99|||||||||
17763|Tanami Group|64277|6|Mentioned|Map ledgend|Paleoproterozoic|Paleoproterozoic|Includes Killi Killi Formation.||||||
17763|Tanami Group|64662|5|Briefly described|p28, p30 Fig. 3|Orosirian|Rhyacian|Contains the Dead Bullock and Killi Killi Formations. Group intruded by doleritic sills and deformed by the ~1830Ma Tanami Event. Geological Province: Tanami region.||||||07-FEB-11
17763|Tanami Group|64675|5|Briefly described|p10, Fig.2, p12, p13, p16, p22, p23, p24|Paleoproterozoic|Paleoproterozoic|Represents a passive margin sequence.|||Includes Killi Killi Formation, Twigg Formation and Dead Bullock Formation. See also Map 2|||19-MAR-14
17763|Tanami Group|64722|5|Briefly described|Fig. 2 p3-6,p10|Orosirian|Orosirian|Tanami Region. Age given by Blake et al. (1975) and Cross and Crispe (2007).|1840 Ma.||Contains Killi Killi Formation.|Unconformably overlies Stubbins Formation, unconformably overlain by Ware Group.|Siliciclastic-dominated metasedimentary rocks|11-APR-12
17763|Tanami Group|64725|6|Mentioned|p62|||Regionally intruded by pre-tectonic dolerite sills that locally have peperitic upper and lower margins.|||Includes Dead Bullock and Killi Killi Formations.|||
17763|Tanami Group|64730|5|Briefly described|p141-142|Paleoproterozoic|Paleoproterozoic|Callie Member includes a felsic tuff dated at 1838 +/- 6 Ma.|||Includes Callie Member [in Dead Bullock Formation].|Unconformably overlies Stubbins Formation.||02-MAY-12
17763|Tanami Group|64733|4|Described|p169, 170 Fig.2, p171, p172, p172 Fig.4|Orosirian|Orosirian|Spatially extensive. Subdivided by Crispe et al. (2007). Age (Crispe et al., 2007) of tuffaceous sandstone in Dead Bullock Formation, but some age uncertainty and may be slightly older than ~1840. Overlies Stubbins Formation. Unconformably overlain by Ware Formation. Intruded by dolerite sills|~1840-1835 from SHRIMP U-Pb zircon.||Includes Dead Bullock Formation and Killi Killi Formation.|Overlies Stubbins Formation. Unconformably overlain by Ware Group.||20-APR-12
17763|Tanami Group|64734|5|Briefly described|p187, p186 Fig.1|Orosirian||Includes Dead Bullock Formation, Killi Killi Formation; intruded by 1825-1790Ma granitic suites and numerous dolerite sills; ages poorly constrained; Au known in all units; largest individual gold deposits in the Group are known in Dead Bullock Formation||||||14-SEP-09
17763|Tanami Group|64735|5|Briefly described|p216 Fig15,|Orosirian|Orosirian|Correlated with Lander Package, Bullion Schist, Ooradidgee Group.||||||30-APR-12
17763|Tanami Group|64737|5|Briefly described|p232, p232 Fig.2, p244|||Intruded by 1820-1800 Ma granites.|~1840 Ma.||Includes Killi Killi Formation.|Overlies Stubbins Formation; unconformably overlain by Birrindudu Group.||01-MAY-12
17763|Tanami Group|65323|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with metadolerite sills and four unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||02-FEB-10
17763|Tanami Group|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with two unnamed units not shown on the map||||||
17763|Tanami Group|65326|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response, which are not shown on this map||||||02-FEB-10
17763|Tanami Group|65327|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response; only one of which is shown on this map||||||
17763|Tanami Group|65328|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and on this sheet, one of four unnamed units differentiated only on the basis of magnetic response||||||02-FEB-10
17763|Tanami Group|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Aileron Province. Includes Killi Killi Formation. Age: older than Tanami Event (1835 Ma)||||||
17763|Tanami Group|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation and two unnamed units one of which is not shown on this map. Mafic volcanics and meta-sediment; interbedded turbiditic sandstone and siltstone||||||
17763|Tanami Group|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as two unnamed units not shown on the map; undifferentiated Tanami Group: interbedded turbiditic sandstone and siltstone||||||02-MAR-10
17763|Tanami Group|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation and 2 unnamed units one of which is not shown on the map. Undifferentiated Tanami Group: interbedded turbiditic sandstone and siltstone. Fine to medium grained metadolerite sills||||||02-MAR-10
17763|Tanami Group|65352|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation along with moderate-highly magnetic metadolerite sills and  3 of 4 unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||
17763|Tanami Group|65353|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic or complex||||||
17763|Tanami Group|65354|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation as well as moderate-highly magnetic metadolerite sills and four unnamed units, differentiated only on the basis of magnetic response, which are not shown on this map||||||02-FEB-10
17763|Tanami Group|65355|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation, Dead Bullock Formation, moderate-highly magnetic metadolerite sills and 2 of 4 unnamed units differentiated only on the basis of magnetic response which varies from non to highly magnetic||||||
17763|Tanami Group|65356|5|Briefly described|Map legend|Orosirian|Archean|Includes Twigg Formation, Killi Killi Formation and Dead Bullock Formation along with moderate-highly magnetic metadolerite sills and four unnamed units differentiated only on the basis of magnetic response; unnamed units not shown on this map||||||
17763|Tanami Group|65358|4|Described|p6-7|Orosirian|Orosirian|In Tanami Region. Overlies Archean basement (Billabong Complex). Unconformably overlain by Ware Group. Includes basal Dead Bullock Formation. Thick metasedimentary succession. 1850-1830 Ma. Deformed during Tanami Event (1840-1825 Ma).||||||19-DEC-16
17763|Tanami Group|65359|6|Mentioned|p1  |||Includes sedimentary rocks of the former Nongra beds.||||||
17763|Tanami Group|66129|6|Mentioned|p214 Fig.1, p216 Fig.3|||Contains Killi Killi Formation and Dead Bullock Formation.||||||
17763|Tanami Group|66468|5|Briefly described|p16-17, p21, p23, p25-27|Orosirian|Orosirian|1864-1844 Ma. Includes Killi Killi and Dead Bullock Formations. Rift architecture. Is overlain by Ware Group.||||||
17763|Tanami Group|66860|6|Mentioned|p6 Tb.1|||Tanami Region. Deposition of lower parts of this unit was coeval with deposition of Lander Rock beds (Arunta Region) and of Warramunga Formation (Tennant Region). The upper parts were deposited at the same time as lower Strangways Metamorphic Complex protoliths and upper parts of Lander Rock beds (Arunta Region) and upper parts of Ooradidgee Group (Tennant Region).||||||
17763|Tanami Group|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Includes Killi Killi and Dead Bullock Formations.|||
17763|Tanami Group|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.|||Includes Dead Bullock and Killi Killi Formations.|||
17763|Tanami Group|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Dead Bullock, Killi Killi and Twigg Formations.|Overlies MacFarlane Peak Group. Intruded by Inningarra, Granites, Frederick, Coomarie, Bore Field Road Suites and Nanny Goat Volcanics. Is unconformably overlain by Birrindudu, Mount Winnecke Groups.||
17763|Tanami Group|67323|5|Briefly described|p29|||Granites-Tanami terrane.|~1850-1835 Ma|||Unconformably overlies Stubbins Formation.||
17763|Tanami Group|67824|5|Briefly described|p383-385, p387, p392-393, p395-396.|Orosirian|Orosirian|Age constrained by constituent Formations. Group thins towards the southeast.|||Includes Killi Killi Formation, Dead Bullock Formation.|Overlies Killi Killi Formation and Billabong Complex. Unconformably overlain by the Ware Group.||
17763|Tanami Group|67826|4|Described|p401 Fig.2, p402, p403||Orosirian|Intruded by extensive granitic magmatism ~ 1820-1790 Ma. Experienced greenschist facies metamorphism and multiple deformation events.|> 1820 Ma||Includes Killi Killi Formation, Dead Bullock Formation.|Unconformably overlain by the Ware Group.||18-SEP-14
17763|Tanami Group|68474|5|Briefly described|p572-574, p576|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. See also Tanami Supergroup. Undergone alteration and greenschist to amphibolite facies metamorphism.|||Includes the Killi Killi Formation, Stubbins Formation and the Dead Bullock Formation.|||
17763|Tanami Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex. Moderate gravity, moderate to highly magnetic.|c.1848-1840 Ma (Huston et al., in press).||Includes Killi Killi Formation.||Metasedimentary rock.|
17763|Tanami Group|68733|5|Briefly described|p186, p187 Fig.6|Statherian|Statherian|Tanami region.||||Uncomformably underlain by the Billabong Complex. Unconformably overlain by the Ware Group. Correlated with Inverway Metamorphics.||06-DEC-17
17763|Tanami Group|68994|6|Mentioned|p6||||||Killi Killi Formation|||
17763|Tanami Group|69003|5|Briefly described|p5, p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Dead Bullock, Killi Killi, Stubbins, Mount Charles Formations.|||
17763|Tanami Group|69253|5|Briefly described|p746-767|Orosirian|Orosirian|Deformation, particularly Trans-Tanami Fault, discussed in detail.|||Includes Dead Bullock and Killi Killi Formations.|Is overlain unconformably by Pargee Sandstone.||
17763|Tanami Group|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.|||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|69417|6|Mentioned|p2:5|Orosirian|Orosirian|Tanami Orogen.||||||12-JUL-16
17763|Tanami Group|69419|6|Mentioned|p4:7,|||Greenschist facies metamorphism.||||||12-JUL-16
17763|Tanami Group|69426|4|Described|p11:1, 3-5, 7-8, 10-11, 13-14, 26-27|Orosirian|Orosirian|Blake et al. (1973); later changed to Tanami Complex (Blake et al., 1975) because of inability to determine the constituent units at that time. Cooper and Ding (1997) used the name Tanami Group for a succession of quartzite, two pelitic units, and metamorphosed turbidites; the quartzite being of sedimentary origin and unconformably overlying the Billabong Complex. Crispe et al. (2007) included the two pelitic units in the Dead Bullock and Killi Killi Formations. Crispe and Vandenberg (2005) regarded the quartzite as (non-sedimentary) thickened, sheared quartz veining. Maximum thickness of 10km in the NW, thinning southwards to 3km. Deformation described in some detail. Age range of 1840-c.1815 Ma is given on p13.|Between c.1864 Ma and c.1821 Ma.||Stubbins, Dead Bullock, Killi Killi Formations.|Is overlain (probably) unconformably by Nanny Goat Volcanics (Ware Group).||12-JUL-16
17763|Tanami Group|69427|6|Mentioned|p12:3|||Tanami Region. Direct stratigraphic correlatives occur in 1860-1830 Ma sedimentary protoliths of metasedimentary rocks in the Aileron Province.||||||12-JUL-16
17763|Tanami Group|69429|6|Mentioned|p14:2|||Tanami Region. A likely correlative of the Inverway Metamorphics (Birrindudu Basin).||||||12-JUL-16
17763|Tanami Group|69432|6|Mentioned|p17:2, 4|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
17763|Tanami Group|69587|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. Tanami Group deposition was terminated by regional deformation and greenschist to amphibolite-facies metamorphism during the Tanami Event at c. 1830 Ma (Bagas et al., 2007). Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|||Includes Dead Bullock Fomation, Killi Killi Formation.|Overlain unconformably by Ware Group.||
17763|Tanami Group|69618|5|Briefly described|p89-93, p95-97, p101 Fig.11, p102 Fig.13|Paleoproterozoic|Paleoproterozoic|See also p107, p109. Was divided into Stubbins Formation (in the west) and Dead Bullock Formation (in the east). The former is now included within the latter. Spread of detrital zircon ages, from Archean to early Paleoproterozoic, is typical of this Group.|c.1840-1835 Ma (Crispe et al., 2007).||Includes Killi Killi, Stubbins, Dead Bullock and Mount Charles Formations.|||
17763|Tanami Group|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
17763|Tanami Group|69747|5|Briefly described|p262,264,267,272|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami Block, North Australian Craton. Most extensive unit across the Granites-Tanami Orogen. Deposited in a back-arc basin environment. Deposition is followed by subductionof the Tanami back-arc oceanic slab which produced enormous subduction-induced heat and resulted in up to amphibolite facies metamorphism in the group. Palaeoproterozoic (ca. 1864 Ma) mafic suites include massive basalt, pillow basalt, basalt breccia and dolerite sills. Also intruded by c. 1800 Ma mafic dykes.|||Includes Killi Killi Formation and Dead Bullock Formation.|||
17763|Tanami Group|69933|6|Mentioned|p11|||||||||
17763|Tanami Group|70024|6|Mentioned|p35|||Folded and sheared by the c.1795 Ma Tanami Orogeny.|c.1865 Ma.||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|70129|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Stubbins Formation.|||
17763|Tanami Group|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Also includes an un-named but separately-mapped unit of feldspathic metawacke, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite and metagabbro.|||Stubbins, Killi Killi Formations.|||
17763|Tanami Group|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1840-1835 Ma.||Killi Killi Formation.||Wacke, feldspathic wacke, quartz sandstone, sandstone, siltstone, mudstone, banded chert, basalt, dolerite and gabbro: all metamorphosed.|
17763|Tanami Group|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1840-1835 Ma.||Killi Killi Formation.|Overlies Stubbins Formation.||
17763|Tanami Group|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Killi Killi Formation.|||
17763|Tanami Group|70291|4|Described|p178-179,181|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Figure 2 p178 suggests that Bald Hill Sequence is part of the Tanami Group, but not so in text. Affected by ~1830 Ma Tanami Event (D1-M1) associated with macrofolding and regional greenschist-amphibolite facies metamorphism.|1838+\-6 Ma||Includes Dead Bullock Formation, Killi Killi Formation, and ?Bald Hill Sequence.|Intruded by dorelite sills, some of which have peperitic contacts with enclosing sedimentary rocks.|Carbonaceous and Fe-rich units.|
17763|Tanami Group|70478|6|Mentioned|p2 Fig 1, 6,10-12|||Geological Province: Tanami.|||Includes unnamed dolerite, Killi Killi Formation and Dead Bullock Formation.||Metasedimentary rocks.|
17763|Tanami Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Tanami Basin, ?Aileron Province.||||||21-APR-20
17763|Tanami Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Undivided: cross-section only; see constituents for further details.|||Dead Bullock, Killi Killi Formations.|Is overlain unconformably by Birrindudu Group.||
17763|Tanami Group|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Dead Bullock, Killi Killi Formations.|||
17763|Tanami Group|71267|4|Described|GEOL_LUT_CSV files|||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, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Killi Killi Formation, Stubbins Formation.||Metamorphosed siliciclastic sedimentary rock and volcanic rocks|
17763|Tanami Group|71349|5|Briefly described|p725|||Crispe et al. (2007).|||Dead Bullock, Killi Killi Formations.|Unconformably overlies Browns Range Metamorphics. Is overlain unconformably by the Ware Group (inferred: contact not exposed). Is intruded by Birthday, Frederick and Grimwade Suites.||
17763|Tanami Group|71397|5|Briefly described|p5,46-47|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen. Broadly a deep-marine succession, dominantly turbiditic (Crispe et al., 2007; Lambeck et al., 2008, 2012; Bagas et al., 2014).|||Includes Killi Killi Formation, Stubbins Formation, Dead Bullock Formation.|Overlain unconformably by Ware Group.||
17763|Tanami Group|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1800+/-14 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
17763|Tanami Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Killi Killi Formation, Stubbins Formation.|||
17763|Tanami Group|73083|6|Mentioned|p23|||Tanami Orogen.|||||Includes metamorphosed rocks.|
17763|Tanami Group|73089|4|Described|p: 1, 3, 5, 7-11, 22-31, 37, 39, 41-44|Paleoproterozoic|Paleoproterozoic|Archean detritus dominates the lower part of the succession, and c. 1865 Ma detritus with a minor c. 2500 Ma component dominates the upper part. Probably also contains Mount Charles Formation. Intruded by granitic rocks. Includes deformation that pre-dates Ware Group. Pre-dates the Stafford Event and are of relatively low metamorphic grade, except near contacts with granitic rocks. Comparable to the Halls Creek Group in terms of lithostratigraphy, changes in provenance and thickness.|||Dead Bullock Formation (Ferdies Member, Callie Member), Killi Killi Formation (NT)|Underlain by Billabong Complex. Unconformably overlain by Ware Group.|Dominantly siliciclastic metasedimentary rocks and lesser chemical metasedimentary and volcanic rocks metamorphosed under greenschist to locally amphibolite facies conditions.|
17763|Tanami Group|73158|5|Briefly described|p2-3, p6 Fig.5, p9-11|Orosirian||Granites-Tanami Orogen. Intruded by multiple generations of dolerite dykes and sills. MacFarlane Peak Group was integrated into the Tanami Group by Ahmed et al., (2013).|>1840 Ma||Dead Bullock Formation, Killi Killi Formation, Stubbins Formation, Mount Charles Formation.||Magmatic and sedimentary rocks. Lower-greenschist metamorphic facies.|
17763|Tanami Group|73159|5|Briefly described|p2-3, p6 Fig.5, p9-11|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. Hosts orogenic gold mineralisation. Intruded by multiple generations of  dolerite dykes and sills.|>1840 Ma.||Dead Bullock, Stubbins, Killi Killi, Mount Charles Formations.|Overlies MacFarlane Peak Group.|Magmatic and sedimentary rocks. Lower greenschist-facies metamorphism.|
17769|Tandalgoo Formation|13255|6|Mentioned|p368|Middle Devonian|Early Devonian|Roebuck Basin.||||Overlies Carribuddy Group. Is overlain by Pillara Reef Complex.||
17769|Tandalgoo Formation|14228|5|Briefly described|p6 fig3|Givetian|Emsian|South Canning Basin.||||Overlies Worral Formation. Overlain by Mellinjerie Formation.||06-OCT-16
17769|Tandalgoo Formation|22753|5|Briefly described|Fig.3 p585|Devonian|Devonian|||||||
17769|Tandalgoo Formation|24061|4|Described|p179|Middle Devonian|Middle Devonian|Geological Province:  Canning Basin.||||||
17769|Tandalgoo Formation|24390|5|Briefly described|p6 Fig. 4|Devonian|Devonian|Geological Province: Canning Basin.||||||
17769|Tandalgoo Formation|40837|3|Fully described|p261|Middle Devonian|Middle Devonian|Informally divided into "Upper Tandalgoo" and "Lower Tandalgoo" equivalent to I and II members, and III and IV members respectively of Koop(1966). Overlain by Dominic Shale. Type section: Sahara No. 1 drill core. See also Fig. 5 page insert (p258).||||||01-FEB-10
17769|Tandalgoo Formation|40992|6|Mentioned|Fig.11|||||||||
17769|Tandalgoo Formation|41276|6|Mentioned|p72|||||||||
17769|Tandalgoo Formation|42933|5|Briefly described|Fig.94 p258|||||||||
17769|Tandalgoo Formation|43563|6|Mentioned|Fig.2,p6|Eifelian|Emsian|||||||
17769|Tandalgoo Formation|43599|6|Mentioned|p248|||||||||
17769|Tandalgoo Formation|43656|6|Mentioned|Fig.2,p8|Givetian|Pragian|||||||
17769|Tandalgoo Formation|43666|6|Mentioned|p20|Eifelian|Emsian|||||||
17769|Tandalgoo Formation|43746|6|Mentioned|Fig.2,p11|Givetian|Emsian|||||||
17769|Tandalgoo Formation|43815|6|Mentioned|p93||Devonian|||||||
17769|Tandalgoo Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
17769|Tandalgoo Formation|50085|5|Briefly described|p6 Fig. 4|Devonian|Devonian|Geological Province: Canning Basin.||||||
17769|Tandalgoo Formation|61020|6|Mentioned|p33 Fig. 4|||Lead for petroleum potential.  Geological Province: Canning Basin.||||||20-APR-05
17769|Tandalgoo Formation|61023|5|Briefly described|p10 Fig. 6|Devonian|Devonian|Geological Province: Canning Basin.||||||11-APR-08
17769|Tandalgoo Formation|64185|5|Briefly described|p158 Fig. 2, p165|Middle Devonian|Middle Devonina|Underlain by Carribuddy Formation, overlain conformably by Lennard River Group. Geological Province: Canning Basin. Aeolian. See p165 for more information.||||||
17769|Tandalgoo Formation|64186|5|Briefly described|p171|Early Devonian|Early Devonian|Underlain by Carribuddy Formation, conformably. Aeolian red beds.||||||
17769|Tandalgoo Formation|64982|5|Briefly described|p699 Fig.4.|Eifelian|Pragian|Up to 400 m thick. Fish scales indicate Early Devonian age; conodonts and spores suggest Givetian-Frasnian age.||||Unconformably overlies Worral Formation.|Red-brown aeolian sandstones.|
17769|Tandalgoo Formation|65214|6|Mentioned|p277|Devonian|Devonian|QLD, Broken River and Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17769|Tandalgoo Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Devonian|Middle Devonian|Disconformably overlies Worral Formation. Geological province: Canning Basin. Non-marine sediments - including reservoir sandstones. See also p8 Fig. 5.||||||
17769|Tandalgoo Formation|65449|5|Briefly described|p1, p5-11, p14, p31-33, p35, p47-48, p51|Middle Devonian|Early Devonian|See also p54; Plates 1-4, 9-11. Base of Megasequence II of Warris (1993). Appears as Tandalgoo Sandstone on p6 and Plate 1. Closely resembles Mereenie Sandstone lithologically. Revised top and thickness data.||Tanndulla Group.||Overlies Worral Formation, probably unconformably. Is overlain conformably by Mellinjerie Formation.|Typically comprising orange to reddish, well-sorted, well rounded, and porous sandstone; mostly eolian with minor fluvial or other facies.|
17769|Tandalgoo Formation|66949|5|Briefly described|p67-68,82 Appx.5|||Mentioned in discussion of Acacia 2 well.||||Is overlain unconformably by Hoya Formation.|Includes sandstone.|
17769|Tandalgoo Formation|68007|4|Described|p1-2, p4-7, p10,p12, p14-15, Plates 1, 2|Middle Devonian|Early Devonian|Canning Basin. ?173m thick in Patience 2 well. Good to excellent reservoir potential. Cuttings from the Patience 1 exploration well yielded a very small amount of liquid hydrocarbon and a black tarry substance: "possible dead oil"; no shows in Patience 2 well. Composite well log. May be effectively sealed by the Clapp Ridge Formation. Eolian to fluvial, with minor marine, deposits. Informal "upper" Tandalgo [stet] Formation shown in Plate 1 and informal 'upper Tandalgoo' Formation mentioned p10.||||Disconformably overlies Worral Formation. Is overlain unconformably by Clapp Ridge Formation.|Includes porous and permeable, pale brown, slightly ferruginous, fine- to medium-grained sandstones with minor interbeds of ferruginous dolomitic siltstone.|24-FEB-20
17769|Tandalgoo Formation|68902|6|Mentioned|p9|Middle Devonian|Early Devonian|||||Overlain by Mellinjerie Formation and Grant Group.||
17769|Tandalgoo Formation|69182|5|Briefly described|Ch4 p9, Ch4 p13-p14, Ch4 p30-p35|Devonian|Devonian|Canning Basin. Excellent reservoir potential for the storage of carbon dioxide with porosities up to 30 percent and permeability reaching several Darcys. See also Ch4 p38-p39, Ch4 p42, Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p65, Ch4 p74, Ch4 p78, Ch4 p84.||||Overlies the Worral Formation. Overlain by the Clapp Ridge Formation.|Red aeolian sandstone.|
17769|Tandalgoo Formation|69312|5|Briefly described|p3, p19, p23 fig 26|Eifelian|Emsian|Canning Basin. See also  p24 fig 28-29, p27 fig 34, p28 fig 35.||||Unconformably (or disconformably) overlies the Worral Formation. Overlies the Sahara Formation. Overlain by the Gogo Formation.|Sandstone.|
17769|Tandalgoo Formation|70774|5|Briefly described|p4|Middle Devonian|Early Devonian|Willara and Kidson Sub-basins, Canning Basin.||||Unconformably? overlies the Worral Formation. Overlain by the Mellinjerie Formation. Equivalent to the Poulton Formation.||10-FEB-20
17769|Tandalgoo Formation|71146|5|Briefly described|p6|Emsian|Lochkovian|Canning Basin.||||Overlies the Worral Formation. Overlain by the Clapp Ridge Formation.|Sandstone.|
17769|Tandalgoo Formation|71618|6|Mentioned|p130|||Of Canning Basin.||||||
17769|Tandalgoo Formation|71894|5|Briefly described|p4, p20|Middle Devonian|Early Devonian|Kidson Sub-basin, Canning Basin.||||Overlies the Worral Formation. Overlain by the Clapp Ridge Formation.|Sandstone.|10-FEB-20
17769|Tandalgoo Formation|72497|5|Briefly described|p3 Fig.2.|Givetian|Emsian|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.||||Conformably underlies Mellinjerie Formation. Laterally equivalent to Worral Formation. Unconformably overlies Sahara Formation.||
17769|Tandalgoo Formation|72499|5|Briefly described|p7 Fig.6.|Middle Devonian|Early Devonian|Located in the Willara Sub-basin and Broome Platform.||||Overlies Worral Formation, conformably to unconformably. Underlies Clapp Ridge Formation.||
17769|Tandalgoo Formation|72504|6|Mentioned|Figure 3|Devonian|Devonian|Canning Basin, Broome Platform. Intersected in Pictor 1 drillhole.||||||18-MAR-20
17769|Tandalgoo Formation|73117|5|Briefly described|p3, p113, p125, p129, p141-142|Middle Devonian|Lower Devonian|Canning Basin. Much of the unit is barren of palynomorphs.||||Underlain by Worral Formation. Overlain by Mellinjerie Formation.|Dominantly sandstone.|
17769|Tandalgoo Formation|73346|6|Mentioned|p3|Middle Devonian|Early Devonian|Canning Basin, southeastern. Contains micro fish material used for age constraint.|||||Eolian, fluvial and minor marine siliciclastic rocks.|
17793|Tanmurra Formation|7142|6|Mentioned|p350 Fig.4.|Early Carboniferous|Early Carboniferous|Browse Basin.||||Overlies Milligans Formation. Is overlain by Point Spring Sandstone.||
17793|Tanmurra Formation|12466|5|Briefly described|p177 Fig.10.|||||||Is overlain by Point Spring Sandstone.||03-SEP-14
17793|Tanmurra Formation|13194|4|Described|p389 Tb. 4-16|Upper Carboniferous|Visean|Type Section: Bonaparte 1 well (194-497m). 100-465m thick deltaic to marine shelf deposits.||Weaber Group||Overlies Milligans Formation (conformably), Bonaparte Formation (unconformably). Part equivalent to Point Spring Sandstone and part equivalent to Burvill Formation.|Calcarenite, dolomite, oolite, sandstone, siltstone, and mudstone.|
17793|Tanmurra Formation|13234|6|Mentioned|p250,252 Figs.2,4; p254; p262 Tb.2 |Early Carboniferous|Early Carboniferous|Encouraging test results for oil fluid and filtrate. Potential reservoir and seal.|||||Includes limestones.|
17793|Tanmurra Formation|13354|6|Mentioned|p375 Fig.6.|Early Carboniferous|Early Carboniferous|Overlies Milligans Formation and underlies Point Spring Sandstone.||66||||28-OCT-14
17793|Tanmurra Formation|14228|6|Mentioned|p6 fig3|Visean|Visean|||||Overlies Millgans Formation||
17793|Tanmurra Formation|22663|5|Briefly described|W97 8 to 10 p2 Fig.3||Carboniferous|||||||01-MAR-10
17793|Tanmurra Formation|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||05-DEC-06
17793|Tanmurra Formation|23820|5|Briefly described|p203|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
17793|Tanmurra Formation|24378|6|Mentioned|p15|||Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|24390|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|24569|5|Briefly described|p248 Fig. 3|Namurian|Visean|Of the Weaber Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
17793|Tanmurra Formation|30550|6|Mentioned|Fig.7|||Lower Carboniferous age||||||
17793|Tanmurra Formation|32307|6|Mentioned|p10|||L.Carboniferous||||||
17793|Tanmurra Formation|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17793|Tanmurra Formation|32663|4|Described|Table 2|||L.Carb.||||||
17793|Tanmurra Formation|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
17793|Tanmurra Formation|32870|5|Briefly described|p48|||||||||
17793|Tanmurra Formation|33621|6|Mentioned|Table 1|||Fossil Shells.||||||
17793|Tanmurra Formation|34085|6|Mentioned|Cor.chart|||Visean - Namurian||||||
17793|Tanmurra Formation|36890|3|Fully described|p381|||||||||
17793|Tanmurra Formation|36904|6|Mentioned|p9|||||||||
17793|Tanmurra Formation|40993|6|Mentioned|Fig.1|||||||||
17793|Tanmurra Formation|41459|6|Mentioned|Fig.2|||||||||
17793|Tanmurra Formation|41532|5|Briefly described|p292|||||||||
17793|Tanmurra Formation|41690|5|Briefly described|p5|||||||||
17793|Tanmurra Formation|41731|5|Briefly described|p573|||See also p519 and Fig.3.||||||05-DEC-06
17793|Tanmurra Formation|41839|4|Described|p32|||||||||
17793|Tanmurra Formation|41864|3|Fully described|p132|||||||||
17793|Tanmurra Formation|41865|5|Briefly described|Map legend|early Namurian|late Visean|||||||
17793|Tanmurra Formation|42055|4|Described|Fig.1 P52|||||||||
17793|Tanmurra Formation|42056|6|Mentioned|p96|||||||||
17793|Tanmurra Formation|42442|3|Fully described|p13|Namurian early|Visean late|||||||
17793|Tanmurra Formation|42547|4|Described|p104|||||||||
17793|Tanmurra Formation|42564|6|Mentioned|p47|||||||||
17793|Tanmurra Formation|43661|6|Mentioned|Fig.3|||||||||
17793|Tanmurra Formation|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
17793|Tanmurra Formation|45038|14|Not recorded|p119|||||||||
17793|Tanmurra Formation|45039|6|Mentioned|p6|||||||||
17793|Tanmurra Formation|45050|6|Mentioned|p57|||||||||
17793|Tanmurra Formation|45056|4|Described|p7|||U.Visean||||||
17793|Tanmurra Formation|45063|6|Mentioned|p8|Early Carboniferous|Early Carboniferous|See also pp22, 27 and Fig. 3.||||||05-DEC-06
17793|Tanmurra Formation|45097|6|Mentioned|p20|||See also correlation chart||||||
17793|Tanmurra Formation|45155|6|Mentioned|p42|||||||||
17793|Tanmurra Formation|45169|4|Described|p7|||||||||
17793|Tanmurra Formation|46849|6|Mentioned|p180|||||||||
17793|Tanmurra Formation|48635|14|Not recorded|Not recorded|||||||||
17793|Tanmurra Formation|48886|14|Not recorded|Not recorded|||||||||
17793|Tanmurra Formation|49637|5|Briefly described|Fig. 6|Late Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||07-FEB-11
17793|Tanmurra Formation|50085|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|60006|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin. Of  Weaber Group. Overlies Milligans Formation. Overlain by Border Creek Member and unconformably overlain by Kuriyippi Formation.||||||
17793|Tanmurra Formation|60364|5|Briefly described|p190, p196|Namurian|Visean|Thickness: 301m. Carbonates and calcareous and dolomitic sandstone. Ostracods described.||||||11-MAY-05
17793|Tanmurra Formation|60682|4|Described|p22 Table. 5, p25|Namurian|Visean|Of Weaber Group. Conformably overlies Milligans Formation. May be equivalent to Point Spring Sandstone and/or Burvill Formation. Thickness: <260m. Sandstone, limestone and dolostone. Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|60701|5|Briefly described|p13|Early Carboniferous|Early Carboniferous|Consists of sandy limestones and calcareous sandstones; good oil shows recorded.  Geological Province: Bonaparte Basin.||||||
17793|Tanmurra Formation|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||10-APR-08
17793|Tanmurra Formation|61542|1|Redefined|p276, p277 Fig. 2, p285|Visean|Visean|Of Weaber Group. Mory's original shelf carbonates unit (1991) is redefined with the upper 26m placed separately in the Sunbird Formation. Unconformable on Kingfisher Shale. Geol.prov: Bonapart Basin/Petrel-Sub-basin.Calcareous and dolomitic sandstone.||||||07-FEB-11
17793|Tanmurra Formation|62837|5|Briefly described|Stratigraphic columns|Namurian|Visean|Of the Weaber Group.  Age: ~328-~322Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
17793|Tanmurra Formation|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
17793|Tanmurra Formation|64694|5|Briefly described|p234, p235, p238 Tb.1, p242 Tb.4, p244|Serpukhovian|Visean|See also p245 Fig.9, p249. Onshore Bonaparte Basin.||Unit in Weaber Group.||Overlies Bonaparte Formation and Upper Milligans Formation unconformably. Is overlain by Point Spring Sandstone or Kulshill Group.||
17793|Tanmurra Formation|65331|6|Mentioned|cross-section only|||?Of Weaber Group.?Carboniferous. Based on colour used. Shown only as subsurface on cross-section||||||
17793|Tanmurra Formation|65342|5|Briefly described|p14. |||Bonaparte Basin. Max. thickness at least 276 m.||||Overlies Milligan Formation. Is overlain by Kulshill Formation.|Sandy limestone, calcareous sandstone.|
17793|Tanmurra Formation|65382|6|Mentioned|p717 App. 2|Namurian|Visean|Bonaparte Basin. 327 Ma.||||||
17793|Tanmurra Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes grey siltstone.|
17793|Tanmurra Formation|67200|6|Mentioned|app 2 p8||||||||Siltstone.|
17793|Tanmurra Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
17793|Tanmurra Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
17793|Tanmurra Formation|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
17793|Tanmurra Formation|69452|3|Fully described|p36:9, 11-12, 14-17|Early Carboniferous|Early Carboniferous|Caye (1968). Equivalent to Medusa Beds of Kemp et al. (1977). Petrel Sub-basin, Bonaparte Basin. The type section is in Bonaparte-1 where it is 277m thick. Transgressive, delta to shallow marine shelf deposits. Offshore and onshore (subsurface). Late Visean.||Weaber Group.||Unconformably overlies Kingfisher Shale and Burvill Formation. Is overlain unconformably by Sandbar and Point Spring Sandstones, Arco and Sunbird Formations.|Calcareous and dolomitic sandstone with minor limestone, siltstone and shale.|12-JUL-16
17793|Tanmurra Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
17793|Tanmurra Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Kingfisher Shale. Is overlain by Sandbar Sandstone.||
17793|Tanmurra Formation|69673|5|Briefly described|p168 fig 138, p171, p172, p181|Carboniferous|Carboniferous|277m thick.||Weaber Group||Overlies Kingfisher Shale, overlain by Kuriyippi Formation, Point Spring Sandstone|Calcareous and dolomitic sandstone with minor limestone, siltstone and shale.|
17793|Tanmurra Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2-3|Visean|Visean|See also Regional geology: Fig.8, p9, p11-12. Includes hydrocarbon source and reservoir rocks.||Weaber Group.||Overlies Kingfisher Shale. Is overlain by Sandbar Sandstone.|Includes anoxic marine mudstones.|12-JUL-16
17793|Tanmurra Formation|70206|5|Briefly described|cross-section only|Carboniferous|Carboniferous|Age implied by surrounding units.||Weaber Group||||
17793|Tanmurra Formation|73117|6|Mentioned|p11, p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Kingfisher Shale and Burvill Formation. Overlain by Sunbird Formation and Sandbar Sandstone.||
17865|Tarraji Microgranite|23722|4|Described|p10|Proterozoic|Proterozoic|Intrudes Whitewater Volcanics. Geological Province: Hooper Complex.||||||12-AUG-08
17865|Tarraji Microgranite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
17865|Tarraji Microgranite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17865|Tarraji Microgranite|30897|6|Mentioned|p10|||Stratigraphic table||||||
17865|Tarraji Microgranite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17865|Tarraji Microgranite|36885|4|Described|p174|||||||||
17865|Tarraji Microgranite|42710|5|Briefly described|map legend|Proterozoic||||||||
17865|Tarraji Microgranite|42811|5|Briefly described|p11|||||||||
17865|Tarraji Microgranite|42814|5|Briefly described|p7|||||||||
17865|Tarraji Microgranite|42815|5|Briefly described|map|||||||||
17865|Tarraji Microgranite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
17865|Tarraji Microgranite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex||Intrudes Lennard Granite.|Porphyritic biotite microgranite and microgranodiorite; phenocrysts of K-feldspar, biotite and quartz.|
17865|Tarraji Microgranite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite.||||||07-NOV-08
17865|Tarraji Microgranite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Porphyritic biotite micromonzogranite|
17865|Tarraji Microgranite|72437|5|Briefly described|p36|||Whole-rock analyses are provided.|||||Monzogranite porphyry.|
17868|Tarrara Formation|13194|4|Described|p395 Tb. 4-16; p382, 399 figs 4-59,-63|Middle Cambrian|Early Cambrian|Type Section: Tarrara Bar 15o04'S 128o41'E. 60-400m thick shallow marine deposits. Includes Blatchford Formation"" (in part).||Unit in Carlton Group.||Overlies Antrim Plateau Volcanics (conformably). Overlain by Hart Spring Sandstone (conformably). Equivalent to Negri Subgroup (Ord Basin).|Siltstone; minor sandstone and limestone.|
17868|Tarrara Formation|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlain by Hart Spring Sandstone.||06-OCT-16
17868|Tarrara Formation|24390|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin. Of the Carlton Group.||||||
17868|Tarrara Formation|32648|6|Mentioned|p32|||M.Camb.||||||
17868|Tarrara Formation|32664|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Briefly described in notes.||||||11-DEC-06
17868|Tarrara Formation|32870|6|Mentioned|Fig.6|||Refers Kaulback and Veevers (1969).||||||11-DEC-06
17868|Tarrara Formation|36257|6|Mentioned|Table 2.1|||||||||
17868|Tarrara Formation|36551|6|Mentioned|Table 16|||||||||
17868|Tarrara Formation|36890|3|Fully described|p374|||||||||
17868|Tarrara Formation|40993|6|Mentioned|Fig.1|||||||||
17868|Tarrara Formation|41459|6|Mentioned|Fig.2|||||||||
17868|Tarrara Formation|41690|5|Briefly described|p3|||||||||
17868|Tarrara Formation|41731|6|Mentioned|Fig.3|||||||||
17868|Tarrara Formation|41864|3|Fully described|p30|||||||||
17868|Tarrara Formation|41865|5|Briefly described|Map Legend|Middle Cambrian||||||||
17868|Tarrara Formation|43661|6|Mentioned|Fig.3|||||||||
17868|Tarrara Formation|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
17868|Tarrara Formation|45038|14|Not recorded|Fig 21,23,36||Cambrian|||||||
17868|Tarrara Formation|45058|6|Mentioned|Fig. 3|||See also Fig. 4. Mid.Cambrian||||||
17868|Tarrara Formation|48886|2|Defined|p.36||Middle Cambrian|See also Figs and App.2, p.61. Middle Cambrian.||||||11-DEC-06
17868|Tarrara Formation|50085|5|Briefly described|p2 Fig. 2|Cambrian|Early Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||15-DEC-08
17868|Tarrara Formation|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||11-APR-08
17868|Tarrara Formation|64443|6|Mentioned|p40.|||Of Bonaparte Basin. Correlative of Barkly Group, Georgina Basin.||||||
17868|Tarrara Formation|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
17868|Tarrara Formation|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Bonaparte Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
17868|Tarrara Formation|67860|6|Mentioned|p419 Tb. 4-18|||Of Bonaparte Basin.||||||
17868|Tarrara Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
17868|Tarrara Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
17868|Tarrara Formation|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Carlton Sub-basin, Bonaparte Basin, Centralian B Superbasin. Sequence 1.||Carlton Group.||Is overlain by Hart Spring Sandstone. Equivalent to Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Walbiri, Giles Creek Dolostones.||12-JUL-16
17868|Tarrara Formation|69443|6|Mentioned|p28:21|||Bonaparte Basin.||||Correlated with Barkly Group.||12-JUL-16
17868|Tarrara Formation|69445|5|Briefly described|p30:17|Middle Cambrian|Middle Cambrian|Bonaparte Basin.||||Unconformably overlies Kalkarindji Suite.||12-JUL-16
17868|Tarrara Formation|69448|6|Mentioned|p33:3|||Bonaparte Basin.||Carlton Group.||Correlated with Negri Subgroup (Ord Basin).||12-JUL-16
17868|Tarrara Formation|69452|5|Briefly described|p36:5|Stage 5|Stage 4|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Unconformably overlies Antrim Plateau Volcanics. Is overlain conformably by Hart Spring Sandstone.||12-JUL-16
17868|Tarrara Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
17868|Tarrara Formation|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian|||Carlton Group||Overlies Antrim Plateau Volcanics, overlain by Hart Spring Sandstone||
17902|Tawallah Group|7071|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|22432|5|Briefly described|p20|||In the McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22453|5|Briefly described|p 11|||||||||
17902|Tawallah Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
17902|Tawallah Group|22538|4|Described|P707, P714|Statherian|Orosirian|Part of the Redbank package||||||06-JUN-18
17902|Tawallah Group|22644|5|Briefly described|3,4,7,9,12,13|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22664|6|Mentioned|35|Paleoproterozoic|Paleoproterozoic|Geological province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|22665|6|Mentioned|P222|||||||||
17902|Tawallah Group|22670|6|Mentioned|53,54,56,58,59,60|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22673|6|Mentioned|64|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22853|4|Described|5|Proterozoic|Proterozoic|Geol province McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23195|6|Mentioned|p5|||Informally referred to "Upper" Tawallah Group.||||||
17902|Tawallah Group|23197|6|Mentioned|Fig.1, p850|||Informally referred to as lower and upper Tawallah Group.||||||
17902|Tawallah Group|23374|6|Mentioned|p8,41,42,34,6,8,30||Statherian|Equivalent to Kombolgie Subgroup. Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23395|4|Described|p384 Fig.2|||||||||
17902|Tawallah Group|23396|5|Briefly described|p407 Fig.2|||||||||
17902|Tawallah Group|23397|6|Mentioned|p471|||||||||
17902|Tawallah Group|23398|5|Briefly described|p436|Statherian|Statherian|||||||
17902|Tawallah Group|23406|5|Briefly described|p601 Fig.3|||||||||
17902|Tawallah Group|23407|5|Briefly described|p627 Fig.2|||||||||
17902|Tawallah Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
17902|Tawallah Group|23776|5|Briefly described|p704|||||||||
17902|Tawallah Group|23809|5|Briefly described|p27|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Tomkinson Creek Group (Ashburton Province) and Birrindudu Group (Birrindudu Basin), and the Wauchope and Hanlon Subgroups of Hatches Creek Group (Davenport Province).||||||
17902|Tawallah Group|23867|5|Briefly described|p14|||See also Fig. 30.  Geological  Province: McArthur Basin.||||||
17902|Tawallah Group|23910|4|Described|p290|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23937|6|Mentioned|p4 Fig. 4, p51|||||||||
17902|Tawallah Group|23963|4|Described|p1237, 1239 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin. Age: 1857+/-30 Ma. Overlies the Scrutton Volcanics.||||||07-NOV-08
17902|Tawallah Group|23968|6|Mentioned|p1346 Fig. 1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: 1800-1700Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|24048|6|Mentioned|p6|||Geological Province: McArthur Basin||||||
17902|Tawallah Group|24050|6|Mentioned|p12|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24197|6|Mentioned|p54|||Contains igneous suites of rocks which are either bimodal, dominantly felsic or dominantly mafic. Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Hobblechain Rhyolite, Selgal Volcanics and Westmoreland Conglomerate.   Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
17902|Tawallah Group|24432|6|Mentioned|p559|||||||||
17902|Tawallah Group|30272|6|Mentioned|p5|||On stratigraphic table||||||
17902|Tawallah Group|30318|6|Mentioned|p327|||||||||
17902|Tawallah Group|30344|6|Mentioned|p29|||See also Fig.4||||||
17902|Tawallah Group|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
17902|Tawallah Group|30508|6|Mentioned|p94|||Stratigraphy||||||
17902|Tawallah Group|30534|6|Mentioned|p306|||||||||
17902|Tawallah Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|31824|6|Mentioned|p28|||Middle Proterozoic||||||
17902|Tawallah Group|32339|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32479|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32519|6|Mentioned|p340|||||||||
17902|Tawallah Group|32658|4|Described|Table 2|||See also Fig.3||||||
17902|Tawallah Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|32660|4|Described|Table 4|||||||||
17902|Tawallah Group|32904|6|Mentioned|p89|||||||||
17902|Tawallah Group|33214|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|33665|5|Briefly described|p366|||||||||
17902|Tawallah Group|34287|6|Mentioned|p34|||||||||
17902|Tawallah Group|34754|6|Mentioned|p15|||||||||
17902|Tawallah Group|35114|6|Mentioned|p203|||||||||
17902|Tawallah Group|35162|6|Mentioned|p1007|||||||||
17902|Tawallah Group|35261|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|35495|6|Mentioned|p340|||||||||
17902|Tawallah Group|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|35776|6|Mentioned|p814|||See also Table 1.||||||
17902|Tawallah Group|35950|6|Mentioned|p311|||||||||
17902|Tawallah Group|36012|3|Fully described|Table 2|||||||||
17902|Tawallah Group|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|37217|6|Mentioned|p650|||||||||
17902|Tawallah Group|37372|6|Mentioned|p2|||||||||
17902|Tawallah Group|37462|4|Described|Table4.IV|||||||||
17902|Tawallah Group|37565|5|Briefly described|p3|||See also Fig.5.||||||11-DEC-06
17902|Tawallah Group|37568|4|Described|p75|||||||||
17902|Tawallah Group|37569|6|Mentioned|p91|||||||||
17902|Tawallah Group|38042|6|Mentioned|p160|||||||||
17902|Tawallah Group|38156|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|38529|6|Mentioned|p275|||||||||
17902|Tawallah Group|38582|6|Mentioned|p215|||||||||
17902|Tawallah Group|38584|4|Described|p10|||||||||
17902|Tawallah Group|38902|6|Mentioned|p20|||||||||
17902|Tawallah Group|39122|6|Mentioned|p154|||||||||
17902|Tawallah Group|39210|5|Briefly described|p50|||||||||
17902|Tawallah Group|39445|6|Mentioned|p36|||See also p39.||||||11-DEC-06
17902|Tawallah Group|39497|6|Mentioned|Fig.4|||||||||
17902|Tawallah Group|39561|6|Mentioned|Fig.5|||||||||
17902|Tawallah Group|39685|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|39925|6|Mentioned|p337|||||||||
17902|Tawallah Group|40105|6|Mentioned|p310|||See also Fig.7||||||
17902|Tawallah Group|40109|5|Briefly described|p302|||||||||
17902|Tawallah Group|40259|6|Mentioned|Table 1|||||||||
17902|Tawallah Group|40489|6|Mentioned|p89|||||||||
17902|Tawallah Group|40491|6|Mentioned|p79|||||||||
17902|Tawallah Group|40691|3|Fully described|p7|||||||||
17902|Tawallah Group|40840|6|Mentioned|Map legend|||||||||
17902|Tawallah Group|40973|6|Mentioned|p193|||||||||
17902|Tawallah Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|41019|5|Briefly described|p243|||||||||
17902|Tawallah Group|41125|6|Mentioned|p35|||||||||
17902|Tawallah Group|41220|5|Briefly described|p366|||||||||
17902|Tawallah Group|41268|4|Described|p283|||||||||
17902|Tawallah Group|41277|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|41319|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41721|3|Fully described|p8|||Comprises 10 named units and is the oldest group in the McArthur Basin sequence. Overlies igneous and metamoprhic complexes of the Murphy Inlier; disconformably overlain by Masterton Sandstone. Geological province: McArthur Basin.||||||01-AUG-07
17902|Tawallah Group|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41957|6|Mentioned|p68|||||||||
17902|Tawallah Group|42385|3|Fully described|p5|Paleoproterozoic|Paleoproterozoic|Includes Yiyintyti Sst, Seigal Volc, Sly Creek Sst, Aquarium Fm, Wununmantyala Sst, Settlement Creek Volcs, Wollogorang Fm, Gold Creek Volcs, Warramana Sst and Tanumbirini Rhyolite. Age between 1857 +/- 30Ma and 1725 +/- 40 Ma. Composite thickness: >5km.||||||06-JUN-18
17902|Tawallah Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|42395|6|Mentioned|Fig.26 P86|||||||||
17902|Tawallah Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||10 fm, 1 mbr. Yiyintyi Ss, Seigal Volcs, Sly Creek Ss (Rosie Creek Ss Mbr), Aquarium Fm, Wununmantyala Ss, Settlement Ck Volcs, Wollogorang Fm, Gold Ck Volcs, Warramana Ss, Tanumbirini Rhyolite.|Underlies McArthur Group.||06-OCT-11
17902|Tawallah Group|42639|3|Fully described|p8, Table 4 p11|Mesoproterozoic||||||||
17902|Tawallah Group|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
17902|Tawallah Group|42739|5|Briefly described|map legend|Statherian|Statherian|Quartz sandstone, conglomerate, mudstone, basaltic and rhyolitic volcanics, minor dolostone.||||||19-OCT-05
17902|Tawallah Group|42753|6|Mentioned|p2|||||||||
17902|Tawallah Group|42812|4|Described|p10, Table 3|||||||||
17902|Tawallah Group|42846|5|Briefly described|p503|||Geological Province: McArthur Basin.||||||09-MAY-05
17902|Tawallah Group|42873|5|Briefly described|p109|||see also Fig.1, p110.||||||11-DEC-06
17902|Tawallah Group|42935|5|Briefly described|p527|||||||||
17902|Tawallah Group|43010|6|Mentioned|p91|||of "Mid Proterozoic" age.||||||
17902|Tawallah Group|43036|4|Described|p13|||||||||
17902|Tawallah Group|43107|6|Mentioned|p9|||||||||
17902|Tawallah Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|43595|4|Described|p438||Mesoproterozoic|||||||
17902|Tawallah Group|43615|6|Mentioned|p14|||||||||
17902|Tawallah Group|43788|6|Mentioned|p13||Proterozoic|||||||
17902|Tawallah Group|44112|6|Mentioned|p10,43|||Part of Supersequence 1(B); middle and upper units in 1(C); upper units in 1(D)||||||
17902|Tawallah Group|44155|6|Mentioned|p252|||McArthur Basin. Probable part correlative of Mount Parker Sandstone and Bungle Bungle Dolomite.||||||
17902|Tawallah Group|44287|14|Not recorded|p.6-16|||(E53-3).||||||
17902|Tawallah Group|44288|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
17902|Tawallah Group|44305|14|Not recorded|p.11-13,18|||(E53-8). opp.p.6,18.||||||
17902|Tawallah Group|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44332|14|Not recorded|p.7,11,12,opp.6,map|||(D53-14).||||||
17902|Tawallah Group|44333|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44434|14|Not recorded|opp.p.6,map|||Correlated with Groote Eylandt Beds. (D53-11,12).||||||
17902|Tawallah Group|44435|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17902|Tawallah Group|44436|5|Briefly described|p.6-10,opp.p.7,map|||(E53-4).||||||02-DEC-04
17902|Tawallah Group|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Includes the Masterton, Wollogorang and Aquarium Formations, and the Settlement Creek Volcanics.||||||07-NOV-08
17902|Tawallah Group|44459|14|Not recorded|p.6,7,opp.p.6, map|||(E53-2). Here includes Rosie Creek Sandstone, Settlement Creek Volcanics, Wollogorang Formation, Masterton Formation (top). See p.12,13, for more details.||||||
17902|Tawallah Group|44460|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44471|14|Not recorded|p.7|||(D53-10).||||||
17902|Tawallah Group|44473|14|Not recorded|p.7-8,13-15,opp. p.7|||(E53-7).||||||
17902|Tawallah Group|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44482|14|Not recorded|p.7|||(E53-12).||||||
17902|Tawallah Group|44530|14|Not recorded|p.4-17|||(D53-15).||||||
17902|Tawallah Group|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|45032|14|Not recorded|p9||Carpentarian|Tb.1, Pl.1.||||||
17902|Tawallah Group|45140|6|Mentioned|p12-13|||McArthur Basin region.|~1575 Ma.|||||
17902|Tawallah Group|45162|2|Defined|p11|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|45166|6|Mentioned|p14|||||||||
17902|Tawallah Group|45167|5|Briefly described|Fig.27|||||||||
17902|Tawallah Group|46804|6|Mentioned|p154|||||||||
17902|Tawallah Group|46861|6|Mentioned|p2|||||||||
17902|Tawallah Group|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
17902|Tawallah Group|46955|6|Mentioned|p159|||||||||
17902|Tawallah Group|46968|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|49001|6|Mentioned|p4|||||||||
17902|Tawallah Group|50225|5|Briefly described|p407|||Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|50591|5|Briefly described|p1.1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|60483|4|Described|p6, p7 Fig. 5|Paleoproterozoic|Paleoproterozoic|Unconformable over basement units including Scrutton Volcanics, and McArthur Group. Max.age: ~1850Ma; min.age: 1713+/-7Ma. Geol.Prov: McArthur Basin. Dominated by shallow marine to fluvial sandstone, with lesser mudstone, dolostone, igneous rocks.||||||07-NOV-08
17902|Tawallah Group|60558|5|Briefly described|p7, p8 Fig. 6, p10, p12|Proterozoic|Proterozoic|Includes 14 units. Coarse-grained terrigenous to shallow marine clasticsand mafic volcanics, with lesser shallow water to shelf carbonates.||||||
17902|Tawallah Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|62084|6|Mentioned|p956||||||||Mafic and felsic volcaniclastic rocks, clastic and minor volcanic rocks.|
17902|Tawallah Group|62285|6|Mentioned|p380, p381|||||||||
17902|Tawallah Group|63110|6|Mentioned|p1141|||Includes; Settlement Creek and Gold Creek Volcanics. Overlain by McArthur Group.||||||11-JUN-08
17902|Tawallah Group|63112|6|Mentioned|p1190, p1992 Tb.1 |||Southern McArthur Basin. Also includes Warramana, Wununmantyala, Rosie Creek, Sly Creek, Echo and Yiyintyi Sandstones and Westmoreland Conglomerate.|||Includes Tanumbirini, Hobblechain Rhyolites; Packsaddle Microgranite; Gold Creek, Settlement Creek, Seigal  Volcanics; Aquarium, McDermott, Nyanantu, Wollogorang Formations. NB: See Comments.|||
17902|Tawallah Group|63866|5|Briefly described|p112, p115|||Southern McArthur Basin.||||Equivalent to the Katherine River Group and the Spencer Creek Group.||
17902|Tawallah Group|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin. Contemporaneous with volcanism in Mount Isa Inlier.|~1795-1695 Ma.||Includes Seigal Volcanics, Gold Creek Volcanics.|||15-MAR-18
17902|Tawallah Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Lower part of this group of the Leichhardt Superbasin (McArthur Basin), deposited during the Leichhardt Extension (1800-1750 Ma). Upper part is part of the Calvert Superbasin, deposited during the Calvert Event (~1730-1690 Ma).||||||
17902|Tawallah Group|64815|5|Briefly described|p3, p4 Fig.2, p5 Fig.3, p6, p10-13|Statherian|Orosirian|See also p15 Fig.9, p16-18 Figs.10-12. Represents the Redbank package. The topmost units are often missing in stratigraphic successions. Appears as Subgroup in Figs.10-12.|Deposition from 1815-1705 Ma.||Includes Yiyintyi, Sly Creek, Warramana, Wununmantyala Sandstones; Seigal, Settlement Creek, Gold Creek, Volcanics; Aquarium, Wollogorang, Nyanantu Formations; Tanumbirini Rhyolite.|Unconformably overlies Scrutton Volcanics.|Composed of sandstone, with bimodal igneous intrusions and lavas, lutite, conglomerate and dolostone.|
17902|Tawallah Group|64817|5|Briefly described|p352 Fig.3, p353 Fig.4, p354, 355, 357|||Also includes Tanumbirini and Hobblechain Rhyolite; Gold Creek, Settlement Creek and Seigal Volcanics. A mid-Tawallah Group east-west compressional event deformed and uplifted older units of the Group.|Shown as ~1790 - <1705 Ma.||Includes Burash, Echo, Warramana, Wununmantyala, Sly Creek and Yiyintyi Sandstones; Westmoreland Conglomerate; Nyanantu, Wollogorang, Aquarium and McDermott Formations; and various volcanic units.|||06-JUN-18
17902|Tawallah Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
17902|Tawallah Group|65228|4|Described|p7, p19, Fig.02|||McArthur Basin. c.5,000 m thick. Lower parts of this unit comprise the Leichhardt Superbasin. Also includes Hobblechain and Tanumbirini Rhyolites.|||Includes Yiyintyi, Sly Creek, Wununmantyala, Warramana Sandstones; Seigal, Settlement Creek, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang Formations; Westmoreland Conglomerate and others.||Shallow water clastics; minor carbonate, shale and volcanic rocks.|
17902|Tawallah Group|65232|5|Briefly described|p9, p20, p78|||Includes Westmoreland Conglomerate at base, Seigal Volcanics, and Wollogorang Formation. Correlatives of Katherine River Group and Tolmer Group. Unconformably overlie northern margin of Murphy Inlier. Uranium deposits. Geol. Prov: McArthur Basin.||||||09-FEB-10
17902|Tawallah Group|65337|6|Mentioned|p6 Fig.3, p15.|||McArthur Basin. Correlative of Carrara Range Group.||||||
17902|Tawallah Group|65340|3|Fully described|p5,  p.13 Table 4, pp11-57, p 66.|||PhD thesis and related papers published (Rawlings 1998, 1999, 2002). Oldest, most areally extensive and voluminous unit in southern McArthur Basin. Forms a regionally extensive, mainly flat-lying platform 2.5 to 6 km thick. Resistant sandstone ranges and plateaux; very little deformation is due to its zone of tectonic stability as well as the structurally competent, thick homogeneous sandstone packages. Probably contiguous with Katherine River Group, Tennant Creek Inlier and Mount Isa Inlier. Contemporaneous with Katherine River, Donydji and Spencer Creek Groups.|||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Burash and Echo Sandstones; Seigal, Gold Creek and other Volcanics; McDermott, Wollogorang and Nyanantu Formations; and more.|Unconformably overlies Murphy and Scrutton Inliers. Is unconformably overlain by McArthur Group,and Karns Dolomite.|Dominated by shallow-marine and fluviatile sandstone, with lesser mudstone, dolostone and bimodal (basalt-rhyolite) volcanic and high-level intrusive rocks.|23-MAR-18
17902|Tawallah Group|66529|5|Briefly described|p21 |||||||Overlies Seigal Volcanics.|Dolomite, sandstone and mafic and felsic volcanic rocks.|
17902|Tawallah Group|66843|5|Briefly described|p23-24|||Oldest tectonic-stratigraphic package in the southern McArthur Basin.|1760 - 1710 Ma.|||Is overlain unconformably by McArthur Group.|Mainly quartz-rich sandstones and mafic to felsic igneous rocks.|
17902|Tawallah Group|67144|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.|||Includes Westmoreland Conglomerate; Seigal, Settlement Creek and Gold Creek Volcanics; McDermott and Wollogorang Formations; Sly Creek Sandstone.|Is overlain by McArthur Group.||13-APR-12
17902|Tawallah Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|||CONSTITUENTS (continued): Gold Creek, Seigal, Settlement Creek, Cliffdale Volcanics.|||Aquarium, McDermott, Wollogorang Formations; Carolina Sandstone Member; Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; Hobblechain Rhyolite. See COMMENTS for more.|||
17902|Tawallah Group|67352|4|Described|v, p11-12, p14-15 Tb.2, p50|Statherian|Statherian|McArthur Basin (Calvert Superbasin). Up to 6 km thick.|1790-1705 Ma||Includes Gold Creek Volcanics, Wollogorang Formation, Settlement Creek Volcanics, Sly Creek Sandstone, McDermott Formation and Seigal Volcanics.|Overlain by McArthur Group (unconformably).|Shallow-marine to fluviatile sandstone and volcanigenic and shallow-intrusive rocks, together with minor lutite, conglomerate and dolostone.|08-JAN-15
17902|Tawallah Group|67564|6|Mentioned|p86.|||Southern McArthur Basin.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|67779|5|Briefly described|p32, p36.|||Southern McArthur Basin. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Spencer Creek Group, Gadabara Volcanics, Groote Eylandt Group and Donji Group.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|McArthur Basin, Mount Isa Province.||||Is overlain conformably by Peters Creek Volcanics.||
17902|Tawallah Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
17902|Tawallah Group|69418|6|Mentioned|p3:15||||||Gold Creek Volcanics.|||12-JUL-16
17902|Tawallah Group|69423|5|Briefly described|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Settlement Creek dolerite, Seigal Volcanics, Westmoreland Conglomerate.|||12-JUL-16
17902|Tawallah Group|69429|5|Briefly described|p14:3|||McArthur Basin.|||Yiyintyi Sandstone.|Unconformably overlies Scrutton Volcanics.||12-JUL-16
17902|Tawallah Group|69430|4|Described|p15:2-4, 9-14, 35, 39, 62|||Southern McArthur Basin. Also includes igneous units: Settlement Creek Dolerite; Hobblechain, Tanumbirini Rhyolites; Packsaddle Microgranite. Generally shallow dipping or flat-lying. May be contiguous with Tomkinson Creek Group (Tomkinson Creek Province) and Haslingden Group (Isa Superbasin). Mentioned as a source of metals for the McArthur River Zn-Pb-Ag deposit. Hosts a number of small U-Au deposits surrounding the Murphy Inlier (described in detail).|>1710 Ma.||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Echo, Burash Sandstones; Seigal, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang, Nyanantu Formations.|Is overlain unconformably by the McArthur and Nathan Groups. Is correlated, and probably contiguous, with the Katherine River Group.|Shallow-marine and fluvial sandstone, with lesser mudstone, dolostone and mafic and felsic volcanic rocks, and coeval and younger intrusive bodies.|12-JUL-16
17902|Tawallah Group|69433|6|Mentioned|p18:1-2, 10|||McArthur Basin.||||Equivalent to Wire Creek Sandstone and Peters Creek Volcanics (Lawn Hill Platform).||12-JUL-16
17902|Tawallah Group|69591|5|Briefly described|p29, p39, p56, p58|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Mount Isa Province. The only unit in the McArthur Basin succession N of the Murphy Tectonic Ridge in Qld.|||Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; McDermott, Aquarium, Wollogorang Formations; Gold Creek, Seigal, Settlement Creek Volcanics; Hobblechain Rhyolite.|||
17902|Tawallah Group|69673|4|Described|p15, p17, p20, p22, p32, p40, p49, p51|Statherian|Statherian|Also includes Tanumbirini Rhyolite, Warramana Sandstone, Hobblechain Rhyolite, Gold Creek Volcanics, Wollogorang Formation, Settlemenet Creek Dolerite, Wununmantyala Sandstone, Aquarium Formation, McDermott Formation, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|1710 Ma||Includes Burash Sandstone, Nyanantu Formation, Echo Sandstone|Correlated with Birrindudu Group|Extensively silicified arkosic or quartz rich sandstone that alternate with mafic volcanic rocks, shale and rare carbonate rocks.|
17902|Tawallah Group|70284|5|Briefly described|p1245|Statherian|Statherian|Leichhardt Superbasin. 1000-4000m thick. Age inferred from age of Leichhardt Superbasin.|||||Fluvial conglomeratic sandstones, mafic volcanics and marine and aeolian sediments.|
17902|Tawallah Group|70302|5|Briefly described|iv, p7|Statherian|Statherian|Southern McArthur Basin. Age is also derived from Page and Sweet, 1998.|c.1730 Ma (Page et al., 2000).|||Correlated with Woodah Sandstone.||05-FEB-18
17902|Tawallah Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic|Chronostratigraphy is adapted from Brasier and Lindsay (1998) and Southgate et al. (2000).|1729 +/- 4 Ma to 1713 +/- 7 Ma.|||Overlain by McArthur Group||06-JUN-18
17902|Tawallah Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin and 'Tawallah Group equivalent' on Lawn Hill Platform. Also includes Packsaddle Microgranite.|||Wire Creek, Sly Creek Sandstones; Peters Creek, Seigal, Settlement Creek, Gold Creek Volcanics; Westmoreland Conglomerate; McDermott, Aquarium, Wollogorang Formations; Hobblechain Rhyolite.|Unconformably overlies Murphy Metamorphics and Cliffdale Volcanics.|Conglomerate, sandstone, greywacke, dolostone; basalt, dolerite, rhyolite, rhyodacite, dacite, trachyte, microgranite.|21-FEB-18
17902|Tawallah Group|70968|6|Mentioned|p2 Fig.3|||||||||
17902|Tawallah Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
17902|Tawallah Group|71374|5|Briefly described|p2, p6|||southern McArthur Basin.|||Includes the Gold Creek Volcanics, Wollogorang Formation and Wununmantyala Sandstone.|Unconformably overlain by the McArthur Group. Equivalent to the lower Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups.||
17902|Tawallah Group|71606|5|Briefly described|p135,137|Statherian|Statherian|Bauhinia Shelf, Batten Trough and Wearyan Shelf, McArthur Basin. Arenite-bimodal volcanic-lutite-carbonate sequence. Age is constrained by 1710-1700 Ma Fagan Phase.|||Includes Hobblechain and Tanumbirini Rhyolites.|Correlable to Groote Eylandt Group. Overlain unconformably by Nathan and McArthur groups, and Karns Dolomite. Correlable to Katherine River Group.||
17902|Tawallah Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally subdivided into lower and upper parts.||||||06-MAR-20
17902|Tawallah Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Quartz sandstone with lesser conglomerate, dolostone, fine-grained clastics, and mafic and felsic volcanics.|
17902|Tawallah Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Birrindudu and Tolmer groups (Birrindudu Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
17902|Tawallah Group|72377|5|Briefly described|iii,p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Wollogorang Formation and Tanumbirini Rhyolite.|||
17902|Tawallah Group|72523|6|Mentioned|p1.|Palaeoproterozoic|Palaeoproterozoic|||||Unconformably underlies the  Nathan Group.||
17902|Tawallah Group|72526|5|Briefly described|p4, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana,  Sandstone, Echo, Wununmantyala, Sly Ck. and Yiyintyi Ss, Nyanantu, Wollogorang, Aquarium and McDermott Fms, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics, Cliffdale Volcanics and Nicholson Granite Complex and unconformably underlying McArthur Group.||
17902|Tawallah Group|72527|6|Mentioned|p1, p3, p5, p7, p176, 185, 193, 194.|Paleoproterozoic|Paleoproterozoic|This group is divided by an unconformity between the earlier Wire Creek Sandstone and Peters Creek Volcanics. Lithographically also contains rounded clasts of predominantly white vein quartz, quartzite, felsic volcanics and rarely, granite.|||Includes Peters Creek Volcanics and Wire Creek Sandstone|Shown as laterally equivalent to and unconformably underlying Carrara Range Group and partially and unconformably overlying Murphy Metamorphics.|Includes feldspathic coarse and coarse-grained, gritty quartz sst., occasionally cross-bedded, with pebble lags and local cobble to boulder congl. lenses.|
17902|Tawallah Group|72718|6|Mentioned|piii, p5, p7|Palaeoproterozoic|Palaeoproterozoic|Beetaloo Sub-basin, McArthur Basin. Calvert/Leichhardt Superbasin, Redbank package. More constituents include the Tanumbirini and Hobblechain rhyolites, Packsaddle Microgranite, Gold Creek and Seigal volcanics, and the Settlement Creek Dolerite.|||Burash, Echo, Warramana, Wununmantyala, Sly Creek, Yiyintyi sandstones; Nyanantu, Wollogorang, Aquarium, McDermott formations; Westmoreland Conglomerate [see comments].|Conformably overlain by Parsons Range Group. Unconformably overlain by McArthur River Group,Nathan Group, Roper Group.|Dominated by shallow-marine to fluvial sandstone, with lesser shale, conglomerate, dolostone and bimodal volcanic rocks.|
17902|Tawallah Group|72912|4|Described|p5 Fig.3, p18-19, p36, p48.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Age constraints from dating of basal Westmoreland Conglomerate at 1815+/-7 Ma (sedimentary depositional age) and Tanumbirini Rhyolite, near top at 1713+/-7 Ma. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana, Echo, Wununmantyala, Sly Creek and Yiyintyi Sandstones, Nyanantu, Wollogorang, Aquarium and McDermott Formations, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics and partially Westmoreland Conglomerate. Shown as unconformably underlying Umbolooga Subgroup, McArthur Group.|Includes sandstone, conglomerate, rhyolite and dolerite.|
17902|Tawallah Group|72919|6|Mentioned|p3, p12|Paleoproterozoic|Paleoproterozoic||||Westmoreland Conglomerate|||
17902|Tawallah Group|72967|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
17902|Tawallah Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert and Leichhardt Superbasin. Constituents: Burash Sandstone, Echo Sandstone, Nyanantu Formation, Tanumbinini Rhyolite, Warramana Sandstone, Pungalina Member, Hobblechain Rhyolite, Gold Creek Volcanics, Settlement Creek Dolorite, Wununmantyala Sandstone, Wuraliwuntya Member, Aquarium Formation, McDermott Formation, Rosie Creek Sandstone Member, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|||See comments.|||
17902|Tawallah Group|73083|6|Mentioned|p35, p37, p40|Paleoproterozoic|Paleoproterozoic||||Seigal Volcanics||Includes a basal sandstone.|
17902|Tawallah Group|73412|4|Described|p1-2, 4, 6-20|||Southern McArthur Basin. Dry bulk density tabulated. Essentially flat-lying stratigraphy. Faults described. Low gravity response; magnetic response is high where volcanic units are preserved; non-conductive unit. Exposed at the surface c.10 km W of the Emu Fault Zone. Mafic volcanics are thought to be the source of Zn and Pb.|1790-1700 Ma.||Yiyintyi Sandstone, Westmoreland Conglomerate, Seigal Volcanics, Wununmantyala Sandstone, Wollogorang Formation, Settlement Creek and Gold Creek Volcanics.|Is overlain unconformably by McArthur Group.|Widespread fluvial to intertidal sandstones and conglomerates and an anomalously thick (c.2 km) pile of mafic volcanics; overlain by shallow marine siliciclastics and carbonates, and volcanics.|
17910|Tchukardine Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
17910|Tchukardine Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Disappointment Group, Officer Basin.||||||
17910|Tchukardine Formation|23590|3|Fully described|p14|Neoproterozoic|Neoproterozoic|<600 Ma. Williams, 1992. Of Disappointment Group. Max. thickness >700 m.||||||
17910|Tchukardine Formation|23602|4|Described|p17|||Of Savory Group.||||||
17910|Tchukardine Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
17910|Tchukardine Formation|23730|4|Described|p13|Neoproterozoic|Neoproterozoic|Of Disappointment Group. O'lying unit Woora Woora Formation. U'lying unit Mundadjini Formation. Geological Province: Officer Basin.||||||
17910|Tchukardine Formation|23760|4|Described|p31|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Geological Province: Officer Basin.||||||
17910|Tchukardine Formation|42708|5|Briefly described|Plate 1|Proterozoic||Reserved as Tchukardine.||||||
17910|Tchukardine Formation|43756|6|Mentioned|Fig.2,p535|||||||||
17910|Tchukardine Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||17-FEB-10
17910|Tchukardine Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
17910|Tchukardine Formation|44111|6|Mentioned|p.58 Fig. 2, p59|||upper Savory Group. The younger part of this unit is equivalent to Supersequence 3 or 4 in Centralian Superbasin.||||||
17910|Tchukardine Formation|61732|5|Briefly described|p85|Ediacaran|Ediacaran|Of the Diasappointment Group. Disconformably or unconformably overlies the Boondawari Formation. Geological Province: Officer Basin.||||||07-FEB-11
17910|Tchukardine Formation|62453|3|Fully described|p5 Fig. 3, 61|Ediacaran|Ediacaran|Geological Province: Paterson Orogen/Officer Basin. Thickness: ~700m. Sandstone, minor siltstone, shale and conglomerate. Unconformably overlies: Mundadjini Formation and Wongarlong Formation. Underlies: Woora Woora Formation disconformably.||||||
17910|Tchukardine Formation|64580|4|Described|map legend||Neoproterozoic|Of Disappointment Group. Medium- to coarse-grained sandstone, quartz wacke, siltstone, and shale; minor conglomerate.||||||09-DEC-08
17910|Tchukardine Formation|64772|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Disappointment Group but not represented in this study area.||||||07-FEB-11
17910|Tchukardine Formation|65410|6|Mentioned|p74.|||Savory Sub-basin. Its stratigraphic position is unclear: Supersequence 3 or 4.||||||
17910|Tchukardine Formation|65416|5|Briefly described|p137, p141, p144, p146.|Early Cambrian|Ediacaran|Officer Basin. Part of Sequence LP4A of Supersequence LP4. Shallow marine shelf.|||||Medium- to coarse-grained sandstone, conglomerate lenses and minor siltstone and shale.|
17910|Tchukardine Formation|65454|4|Described|p7 Fig.3, p11, p30 Fig.A1b|Paleozoic|Cambrian|Of Disappointment Group, Officer Basin. Medium-grained sandstone, with rare intercalations of silty shale, siltstone and conglomerate. Similar to McFadden Formation. Overlies Mundadjini Formation. Disconformably overlain by Woora Woora Formation.||||||21-APR-16
17910|Tchukardine Formation|67202|5|Briefly described|p64, p66|||NW Officer Basin. At least 700m thick. Sandy marine shelf deposits.||Disappointment Group.||Unconformably overlies the Tarcunyah Group.|Consists mainly of medium-grained quartz sandstone, but includes thin basal units of pebble to cobble conglomerate, pebbly sandstone, mudstone and siltstone.|
17910|Tchukardine Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Disappointment Group.||||
17910|Tchukardine Formation|69590|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|||Unit of Disappointment Group.|||Medium- to coarse-grained sandstone, quartz wacke, siltstone, and shale; minor conglomerate|
17910|Tchukardine Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, conglomerate, sandstone|
17910|Tchukardine Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Officer Basin (Phase 1).||Disappointment Group|||Medium- to coarse-grained sandstone, quartz wacke, siltstone, and shale; minor conglomerate.|
18018|Thaduna Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Yerrida Basin. Terrigenous, sedimentary.||Of the Mooloogool Subgroup.|||Lithic sandstone and shale.|
18018|Thaduna Formation|12099|4|Described|p677-9, 680-1, 683, Figs.2, 4, 5, 6|Paleoproterozoic|Paleoproterozoic|Deposited in a high energy environment. Rift-fill facies. Distribution is centred around the Goodin Inlier in a broad northeast-trending belt. Possibly sourced from Archean rocks of the Goodin and Marymia Inliers. Intruded by tholeiitic sills.||Unit in Mooloogool Subgroup.||Conformably overlies Johnson Cairn Formation. Interdigitates with mafic volcanics of the Killara Formation.|Predominantly a turbiditic succession of lithic sandstone, quartz wacke with intercalated siltstone and shale, and subordinate dolomite.|04-MAR-13
18018|Thaduna Formation|22501|6|Mentioned|p117 Fig. 3|||in the Yerrida Province||||||
18018|Thaduna Formation|22940|4|Described|Fig.1 p3|||See also Table 2 p12. of Mooloogool Subgroup, Yerrida Group.||||||
18018|Thaduna Formation|23581|5|Briefly described|Map legend|||Of the Mooloogool Subgroup in the Yerrida Group in the Yerrida Basin||||||
18018|Thaduna Formation|23589|5|Briefly described|p18|||Of Mooloogool Subgroup.||||||
18018|Thaduna Formation|23593|4|Described|p10|||Of Mooloogool Subgroup. Overlain by Doolgunna Formation. Underlain by Johnson Cairn Formation. Geological Province: Yerrida Basin.||||||16-FEB-09
18018|Thaduna Formation|23597|4|Described|p10|||Of Mooloogool Subgroup. Underlying unit Johnson Cairn Formation. Max. thickness: >5000 m.||||||
18018|Thaduna Formation|23600|4|Described|p8|Proterozoic|Proterozoic|Previously Thaduna Greywacke.  Of Mooloogool Subgroup. Underlying unit Johnson Cairn Formation. Geological Province: Yerrida Basin. Max. thickness 5000 m.||||||
18018|Thaduna Formation|23744|5|Briefly described|p10 Table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
18018|Thaduna Formation|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
18018|Thaduna Formation|23749|4|Described|p8|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
18018|Thaduna Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
18018|Thaduna Formation|23798|6|Mentioned|p19|||See also Thaduna Greywacke - names used interchangeably. Geological Province: Yilgarn Craton.||||||05-JUL-06
18018|Thaduna Formation|23865|5|Briefly described|p170|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
18018|Thaduna Formation|23890|5|Briefly described|p21 Fig.11|||Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
18018|Thaduna Formation|24021|3|Fully described|p3|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||10-NOV-15
18018|Thaduna Formation|24028|5|Briefly described|p288|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup.  Geological Province: Yerrida Basin.||||||07-NOV-08
18018|Thaduna Formation|24535|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|Rift fill conglomerates, megabreccias and turbidites. Of the Mooloogool Group. Geological Province: Yerrida Basin.||||Interdigitates with Doolgunna Formation and Killara Formation.||26-NOV-13
18018|Thaduna Formation|42730|5|Briefly described|Fig 12, P15|||||||||
18018|Thaduna Formation|43238|5|Briefly described|p6|||||||||
18018|Thaduna Formation|43836|5|Briefly described|Map Legend||Proterozoic|||||||
18018|Thaduna Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group).  Lithic sandstone and shale; minor dolomite.||||||18-MAY-04
18018|Thaduna Formation|44830|5|Briefly described|Map Legend||Proterozoic|||||||
18018|Thaduna Formation|49893|4|Described|p13|||Of the Mooloogool Subgroup. Geological Province: Yerrida Basin. Conformably overlies the Johnson Cairn Formation. Overlain by the Killara Formation. Supersedes Thaduna Greywacke. Max. thickness: 5km. See also p2 Fig.1.||||||
18018|Thaduna Formation|49896|5|Briefly described|p3 Tb. 2|||Of Windh (1992). Supersedes Thaduna Greywacke. Now of the Mooloogool Subgroup (Yerrida Group).||||||
18018|Thaduna Formation|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Yerrida Group.  Geological Province: Yerrida Basin.||||||
18018|Thaduna Formation|50222|4|Described|p319 Fig. 2, p320 Fig. 3, p321, 3222|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Group.  Predominantly  lithic sandstone, quartz wacke and intercalated siltstone and shale and subordinate dolomite.  Disconformably overlies Johnson Cairn Fm.; interdigitates with Doolgunna and Killara Fms.  Geol.Prov: Yerrida Basin.||||||07-NOV-08
18018|Thaduna Formation|61217|5|Briefly described|p43 Fig. 2A|Proterozoic|Proterozoic|See also Thaduna Greywacke. Of the Bryah Group. Lithic psammites, pelites, wackes.||||||07-FEB-11
18018|Thaduna Formation|61269|6|Mentioned|p87 Fig.2|||||||||19-MAY-06
18018|Thaduna Formation|61271|6|Mentioned|p105 Fig.1|||Of the Mooloogool Subgroup.||||||
18018|Thaduna Formation|62289|4|Described|plate 1, p3-p4, p7-p8, p12, p14-15|Palaeoproterozoic|Palaeoproterozoic|Redefined by Occhipinti et al., 1997; of Mooloogool Subgroup (Yerrida Group); interdigitates with Killara and Doolgunna Formations; lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite. See also Thaduna Beds and Thaduna Greywacke.||||||
18018|Thaduna Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Mooloogool Subgroup, Yerrida Group.||Coeval and interbedded with Killara and Doolgunna Formations.|Undifferentiated siliciclastic sedimentary rocks and chert.|14-APR-11
18018|Thaduna Formation|63866|5|Briefly described|p165-p166|Statherian|Orosirian|Yerrida Basin.|c. 1800 Ma (Pb-Pb, Gee, 1990)|Mooloogool Subgroup|||Turbidite.|
18018|Thaduna Formation|64580|4|Described|map legend||Paleoproterozoic|Of Mooloogool Group. Lithic sandstone; litharenite; shale; siltstone; and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.||||||09-DEC-08
18018|Thaduna Formation|65408|4|Described|pp82-83, p84 Fig.1.|Paleoproterozoic|Paleoproterozoic|Turbidites include tabular blocks from Killara Formation.||Unit in Mooloogool Subgroup.||Intercalated with Killara Formation lavas and sills.|Dominantly turbiditic; lithic wacke, siltstone, shale, minor arkose.|
18018|Thaduna Formation|65411|6|Mentioned|p89 Fig.1.|||||Unit in Mooloogool Subgroup.||||
18018|Thaduna Formation|65412|6|Mentioned|p101 Fig.4.|||||||||
18018|Thaduna Formation|65419|1|Redefined|p4 Fig.1, p10 Fig.3, p18, p19, pp24-25.|Paleoproterozoic|Paleoproterozoic|Originally Thaduna Beds of MacLeod (1970); later Thaduna Greywacke of Gee (1979, 1987); revised in this study. Includes lithologies other than wacke. Includes strata on northern Mount Bartle 1:100 000 sheet, previously included in the Maraloou Formation; also some areas mapped as Doolgunna Formation on southeastern Peak Hill 1:250 000 sheet. Named after the abandoned Thaduna mine site which is also the type area. Thickness uncertain; may be a few kilometres.||Unit in Mooloogool Subgroup.||Overlies Johnson Cairn Formation conformably/transitionally. Interfingers with overlying Doolgunna Formation. Interfingers with Killara Formation. Is conformably overlain by Maraloou Formation.|A turbiditic succession consisting of graded beds of coarse- to fine-grained purple-grey litharenite and wacke, in places feldspathic, with interbedded siltstone and shale.|
18018|Thaduna Formation|65472|5|Briefly described|p2, p3 Fig.2|||Yerrida Basin.||Mooloogool Group|||with Doolgunna Formation, conglomerate and turbidite facies|
18018|Thaduna Formation|65913|4|Described|p2 Fig.1, pp6-8. |Paleoproterozoic|Paleoproterozoic|A complex sequence of turbiditic siliciclastic rocks, locally intercalated with igneous rocks of Killara Formation.||Unit in Mooloogool Subgroup.||Is intercalated with Killara Formation.|Mainly litharenites and quartz wackes; litharenites are fine- to coarse-grained, commonly upward-fining, poorly sorted, often ferruginized, interbeds of siltstone and shale, laminated, subarkosic, with concretions; spheroidal weathered wackes.|
18018|Thaduna Formation|66427|6|Mentioned|p41 Tb.1, p72 Fig.26 |||Deposition of immature sediments from orogenic highlands.||||||
18018|Thaduna Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Mooloogool Group|||Lithic sandstone; litharenite; shale; siltstone; and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite|
18018|Thaduna Formation|69003|5|Briefly described|p11-12|||Yerrida Basin.||Mooloogool Group.||Unconformably overlies Johnson Cairn Formation.||
18018|Thaduna Formation|69152|4|Described|500k_geologyp08_lut||Paleoproterozoic|||Mooloogool Group|||Lithic sandstone; litharenite; shale; siltstone; and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|07-AUG-15
18018|Thaduna Formation|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Mooloogool Group|||Lithic sandstone; litharenite; shale; siltstone; and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18018|Thaduna Formation|69596|6|Mentioned|p9-10|||Yerrida Basin.||Mooloogool Group.||||
18018|Thaduna Formation|70136|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Mooloogool Group.|||Lithic sandstone, litharenite, shale, siltstone and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18018|Thaduna Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2500 - 1600 Ma (inferred).|Mooloogool Group|||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18018|Thaduna Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv,  West Australian Craton, Bryah Basin|2500-1600 Ma||||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18018|Thaduna Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen.|ca 25001600 Ma (inferred)|Mooloogool Group|||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18018|Thaduna Formation|70804|5|Briefly described|p2, p16, p37|||Replaces the obsolete Thaduna Greywacke. The type area is located on the Thaduna map sheet (Pirajno and Adamides, 1998).||Mooloogool Subgroup||||
18018|Thaduna Formation|70814|5|Briefly described|p48|||Bryah Basin.||Bryah Group||Overlies the Narracoota Formation.||
18018|Thaduna Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, crystalline dolostone/dolomite, sandstone, schist, conglomerate|
18018|Thaduna 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.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite|
18018|Thaduna Formation|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Capricorn Orogen. Of Yerrida Basin/Earaheedy Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite|
18018|Thaduna Formation|71468|4|Described|p24-26|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin. Broadly coeval with Killara Formation.||Unit of Mooloogool Group.||Laterally grades into Killara Formation. Time-equivalent to Doolgunna Formation.|Arkosic sandstone, lithic sandstone, quartz wacke, minor conglomerate, siltstone, mudstone and laminated quartz sandstone that locally contain fragments of basaltic scoria.|
18018|Thaduna Formation|71484|5|Briefly described|p125,128-129,134|||Geological province: Of Yerrida Basin. Present in the NE Yerrida Basin adjacent to the Goodin Fault, and the south-central part of the basin.||Unit of Mooloogool Group.||Overlain by Maraloou Formation. Underlain by Killara Formation.|Arkosic and lithic sandstone and quartz wacke; minor congloemrate, siltstone, mudstone and laminated quartz sandstone, locally containing fragments of basaltic scoria.|30-AUG-19
18018|Thaduna Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Mooloogool Group|||Lithic sandstone, litharenite, shale, siltstone, and quartz wacke; locally containing fragments of basaltic scoria and thin volcaniclastic lenses; minor dolomite.|
18020|Thambrong Formation|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Overlying unit: Weedarra Shale. Underlying unit: Mundarie Siltstone. Of the Lyons Group.||||||
18020|Thambrong Formation|36890|6|Mentioned|p279|||||||||
18020|Thambrong Formation|41271|6|Mentioned|p65|||||||||
18020|Thambrong Formation|42392|6|Mentioned|p120|||Lyons Group||||||
18020|Thambrong Formation|44344|14|Not recorded|p.6,8-9,opp.4,map||Sakmarian|Sakmarian; fm. of Lyons Group. (G50-1).||||||
18020|Thambrong Formation|44345|14|Not recorded|map legend||Sakmarian|Sakmarian.||||||
18020|Thambrong Formation|44532|4|Described|p.6, map|||(G50-5).||||||
18020|Thambrong Formation|44533|5|Briefly described|map legend||Sakmarian|Sakmarian.||||||
18020|Thambrong Formation|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group.||||||01-JUN-06
18020|Thambrong Formation|45016|2|Defined|p.43-50||Sakmarian|Tb, p7,12,13,16,40,42,51,52,55,56,57,59-62,69,104,Fig. 52,56,65. (F50-13).||||||
18020|Thambrong Formation|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
18028|Thangoo Calcarenite|22765|6|Mentioned|P9|||||||||
18028|Thangoo Calcarenite|35119|4|Described|p459|||See also mention on P456.||||||
18028|Thangoo Calcarenite|36890|3|Fully described|p325|||||||||
18028|Thangoo Calcarenite|43563|6|Mentioned|p4||Devonian|||||||
18028|Thangoo Calcarenite|44998|2|Defined|p20,60|||Overlain by Grant Formation. Overlies Roebuck Dolomite.||||||
18028|Thangoo Calcarenite|45153|3|Fully described|App.2-31|||See also App.1-20||||||
18028|Thangoo Calcarenite|46973|6|Mentioned|Fig.1|||||||||
18039|The Granites Granite|22716|6|Mentioned|table4, p232|Statherian|Statherian|Age: 1790 Ma.||||||22-DEC-08
18039|The Granites Granite|23363|5|Briefly described|351 Tab.2|Statherian|Orosirian|Age: 1795+/-6Ma.||||||21-SEP-06
18039|The Granites Granite|23599|6|Mentioned|p15|||Geological Province: Granites-Tanami Inlier.||||||22-DEC-08
18039|The Granites Granite|23809|6|Mentioned|p11, p13|Paleoproterozoic|Paleoproterozoic|Age: 1795+/-6Ma (Ozchron, AGSO).||||||07-NOV-08
18039|The Granites Granite|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Of The Granites Supersuite. Geological province: Granites-Tanami Block.||||||07-FEB-11
18039|The Granites Granite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province: Tanami Inlier. Name written as The Granites only under heading for GRANITE.||||||07-NOV-08
18039|The Granites Granite|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18039|The Granites Granite|31362|4|Described|Table 1|||||||||
18039|The Granites Granite|34810|6|Mentioned|p4|||||||||
18039|The Granites Granite|35227|6|Mentioned|Map legend|early Carpentarian|early Carpentarian|||||||
18039|The Granites Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18039|The Granites Granite|39559|6|Mentioned|Table 1|||||||||
18039|The Granites Granite|39888|6|Mentioned|Fig.7|||||||||
18039|The Granites Granite|41465|6|Mentioned|p13|||||||||
18039|The Granites Granite|45140|2|Defined|p12-13, p15, p22-23, p25, p32-35, p37-38|Paleoproterozoic|Paleoproterozoic|See also p46, p74, p78, p83, Appx.p9-10. Hodgson (1976). The Granites-Tanami Block. Named after the abandoned gold mining settlement of The Granites; the type area is 1km S of there at 20deg 34'30"S, 129deg 21'10"E. Generally friable and highly weathered; locally forms tors and spheroidal boulders. Geochemistry detailed. Source of potable borewater at The Granites.|1780 +/- 24 Ma; Rb-Sr whole-rock: Page et al. 1976|||Is overlain by Muriel Range Sandstone. Intrudes Mount Charles Beds (Tanami Complex).|Pink and grey, locally porphyritic, biotite adamellite and associated minor aplite and pegmatite; cross-cutting quartz veins common; local poikilitic alkali feldspar crystals over 1 cm across.|
18039|The Granites Granite|46788|4|Described|p10|||||||||
18039|The Granites Granite|46864|6|Mentioned|p37|||Re age dates||||||
18039|The Granites 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: 1795-1742 +/- 24Ma (Shrimp, Rb-Sr).||||||07-NOV-08
18039|The Granites Granite|61056|5|Briefly described|p778, p779 Tb. 1|Paleoproterozoic|Paleoproterozoic|Age: 1780+/-24Ma (whole rock samples).||||||07-NOV-08
18039|The Granites Granite|61246|5|Briefly described|p3|||Of the Grimwade Suite (?). Foliated monzogranite.||||||11-DEC-06
18039|The Granites Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
18039|The Granites Granite|69426|5|Briefly described|p11:10, 13, 21, 24|Statherian|Statherian|Blake et al. (1979). SHRIMP U-Pb zircon magmatic crystallisation age. An age of 1975 +/- 6 Ma (Smith, 2000) is also given [probably a misprint of 1795 Ma].|1791 +/- 4 Ma (Smith, 2001).|||||12-JUL-16
18039|The Granites Granite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1795+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite, foliated monzodiorite.|
18048|The Sisters Lamproite|41158|6|Mentioned|Table 53|||||||||
18058|Thirindine Formation|29549|6|Mentioned|p145|||Cretaceous||||||
18058|Thirindine Formation|41271|6|Mentioned|p150|||||||||
18058|Thirindine Formation|42123|6|Mentioned|p15|||||||||
18058|Thirindine Formation|42995|5|Briefly described|p15|||||||||
18058|Thirindine Formation|44532|14|Not recorded|p.9|||Formation of Murchison R. area is almost certainly part of Windalia Radiolarite. (G50-5).||||||
18058|Thirindine Formation|45015|5|Briefly described|map legend||Early Cretaceous|Of the Winning Group.||||||01-JUN-06
18058|Thirindine Formation|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||
18064|Thomas Rhyolite|30388|4|Described|Table 1|||Table 1 on P9-10. Middle Proterozoic age.||||||
18064|Thomas Rhyolite|30390|4|Described|p64|||||||||
18064|Thomas Rhyolite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18064|Thomas Rhyolite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18064|Thomas Rhyolite|36551|6|Mentioned|Table 31|||||||||
18064|Thomas Rhyolite|36886|4|Described|p198|||||||||
18064|Thomas Rhyolite|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Bentley Supergroup.||||||
18064|Thomas Rhyolite|67375|5|Briefly described|p20 Fig.11, p38 Table 1, p49. |Mesoproterozoic|Mesoproterozoic|Most laterally continuous rhyolite unit, traceable over the entire extent of the Cassidy Group outcrop area.|1057 +/- 6 Ma.|||Overlies Gurgadi Basalt. Is overlain by Warubuyu Basalt.|Dark-grey, feldspar-phyric rhyolite with very fine-grained groundmass; massive, flow-banded or spherulitic|
18064|Thomas Rhyolite|67553|4|Described|p21,40,51,53-54|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Depositional age at 1057+\-6 Ma (GSWA 174691). Most laterally continuous unit and can be traced over entire outcrop area.|1065+\-5 Ma|Unit of Cassidy Group.||Overlain by Warubuyu Basalt. Underlain by Gurgadi Basalt.||
18064|Thomas Rhyolite|68995|5|Briefly described|p7 Fig.3, p9 Tb. 1, p18, p22, p27 Tb.2|Stenian|Stenian|Estimated 360m thick. Most laterally continuous rhyolite of the Cassidy Group and can be traced over the entire extent of its outcrop. Metamorphism discussed. See also p61.||Cassidy Group||Overlies the Gurgadi Basalt. Overlain by the Warubuyu Basalt.|Rhyolitic lava flows or rheomorphic ignimbrites.|
18064|Thomas Rhyolite|69091|6|Mentioned|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
18064|Thomas Rhyolite|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Middle Cambrian|Bentley Basin, Paterson Orogen. Geochron date 1057+/-6 Ma is interpreted as magmatic crystallization age (see GEOCHRON/174691.1.pdf). Mentioned in GEOCHRON/174690.1.pdf.|1057+/-6 Ma|Cassidy Group|||Porphyritic rhyolite with minor trachyte and dacite; vitric lavas; sample descriptions include: metabasalt, felsic volcanic rock, (feldspar-phyric) rhyolite, rhyodacite|
18064|Thomas Rhyolite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
18064|Thomas Rhyolite|70095|5|Briefly described|p16-17,19,21|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of rhyolitic package: 0.36km, over 90km in strike length and interpreted minimum volume of 970km3. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||Unit of Cassidy Group.||Overlain by Warubuyu Basalt. Underlain by Gurgadi Basalt.||
18064|Thomas Rhyolite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1057 Ma.|Cassidy Group.||Overlies Gombugurra Rhyolite.|Porphyritic rhyolite with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; locally abundant fiamme (section only).|
18064|Thomas Rhyolite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1057 Ma.|Cassidy Group.||Overlies Gurgdi [mis-spelling of Gurgadi] Basalt. Is overlain by Warubuyu Basalt.|Porphyritic rhyolite with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; locally abundant fiamme.|12-NOV-15
18064|Thomas Rhyolite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age obtained from rhyolite sample (file 174691.1.pdf)|1047 Ma - 1077 Ma (Inferred), 1057  (SHRIMP)|Cassidy Group|||Porphyritic rhyolite with minor trachyte and dacite; massive to flow banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; locally abundant fiamme|
18064|Thomas Rhyolite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Sample GSWA 174691 (rhyolite) yielded an interpreted (regression intersecting concordia curve) magmatic crystallisation age of 1057+\-6 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 with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; locally abundant fiamme|
18064|Thomas Rhyolite|71211|6|Mentioned|p216|||||Cassidy Group||||
18064|Thomas 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 174691 (rhyolite) yielded a rgression line intersecting concorcia curve at 1057+|-6 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 with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; locally abundant fiamme|
18064|Thomas Rhyolite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1057+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
18064|Thomas Rhyolite|72443|5|Briefly described|p738-740, p742, p748|||Talbot Sub-basin. Laterally continuous rhyolite unit with an outcrop strike length of >90km.|1032 +/- 26 to 1056 +/- 9Ma (SHRIMP U-Pb)|Cassidy Group|||Rhyolite containing abundant flattened pumice showing flow-foliation that wraps around crystals.|
18105|Throssell Shale|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Mount House Formation.||||||
18105|Throssell Shale|30525|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18105|Throssell Shale|30533|4|Described|Table 5|||Part of Mount House Group||||||
18105|Throssell Shale|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18105|Throssell Shale|30896|4|Described|p19|||||||||
18105|Throssell Shale|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18105|Throssell Shale|32660|5|Briefly described|Table 6|||||||||
18105|Throssell Shale|32728|6|Mentioned|Table 7|||See also Fig.16||||||
18105|Throssell Shale|36551|6|Mentioned|Table 10|||||||||
18105|Throssell Shale|36888|4|Described|p213|||||||||
18105|Throssell Shale|36898|6|Mentioned|p181|||See also p191.||||||03-JUN-08
18105|Throssell Shale|37462|6|Mentioned|p294|||||||||
18105|Throssell Shale|37927|5|Briefly described|p509|||||||||
18105|Throssell Shale|38157|6|Mentioned|Table X|||||||||
18105|Throssell Shale|41429|6|Mentioned|p247|||||||||
18105|Throssell Shale|42710|5|Briefly described|map legend|Proterozoic||||||||
18105|Throssell Shale|42811|5|Briefly described|p31|||of Mount House Group||||||
18105|Throssell Shale|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount House area. 200 m thick.||Mount House Group||Conformably overlies Traine Formation. Is overlain conformably by Estaughs Formation.|Grey-green micaceous, chloritic shale and siltstone.|
18105|Throssell Shale|44366|14|Not recorded|p.17, Table 2||Adelaidean|Part of Mount House Group. Definition on Tech.File E/52-5.||||||
18105|Throssell Shale|44367|14|Not recorded|map legend||Adelaidean|(Reprinted 1971).||||||
18105|Throssell Shale|48927|6|Mentioned|Table 1|||Refers Plumb (in prep.)||||||
18105|Throssell Shale|48931|4|Described|p61|||||||||
18105|Throssell Shale|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Mount House Group.||||
18105|Throssell Shale|67563|6|Mentioned|p120 Fig.1|||||||||
18105|Throssell Shale|68244|4|Described|p660-662|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. Rb-Sr whole-rock age of 671+\-72 Ma (Plumb 1981, recalculated from data obtained by Bofinger 1967).||Unit of Mount House Group.||Overlain by Estaughs Formation. Underlain by Traine Formation.|Fissile shale.|
18105|Throssell Shale|68473|6|Mentioned|p529, 531-535, p547|||Up to 100m thick.||Mount House Group|Equivalent to the Johnny Cake Shale Member.|Equivalent to the upper Ranford Formation.|Dominated by shale with minor fine sandstone interbeds.|
18105|Throssell Shale|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Mount House Sub-basin, Louisa Basin.||Mount House Group|||Blue-grey or grey-green, poorly laminated, micaceous siltstone with minor shale interbeds; coarsening upwards with grey-green, fine-grained, flaggy, laminated, micaceous sandstone interbeds.|04-AUG-15
18105|Throssell Shale|69634|4|Described|GEOL_LUT_CSV files|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 Mount House Group.|||Blue-grey or grey-green, poorly laminated, micaceous siltstone with minor shale interbeds; coarsening upwards with grey-green, fine-grained, flaggy, laminated, micaceous sandstone interbeds|
18105|Throssell Shale|69660|5|Briefly described|Map legend|Ediacaran|Ediacaran|Louisa Basin, North Australian Craton.||Unit in Mount House Group.|||Blue-grey or grey-green, poorly laminated, micaceous siltstone with minor shale interbeds; coarsening upwards with grey-green, fine-grained, flaggy, laminated, micaceous sandstone interbeds.|
18105|Throssell Shale|70154|4|Described|250k_geologyp_lut.csv|Ediacaran|Ediacaran|See also 250k_interpgeop_lut.csv.|541-635 Ma|Mount House Group|||Blue-grey or grey-green, poorly laminated, micaceous siltstone with minor shale interbeds; coarsening upwards with grey-green, fine-grained, flaggy, laminated, micaceous sandstone interbeds|
18105|Throssell Shale|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|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 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|635-541 Ma (inferred)|Unit of Mount House Group.|||Blue-grey poorly laminated micaceous siltstone with minor shale interbeds; sandy in the upper parts with fine grained flaggy grey-green laminated micaceous sandstone interbeds|
18105|Throssell Shale|71811|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Louisa Basin.||Mount House Group.|||Blue-grey or grey-green, poorly laminated, micaceous siltstone and shale; coarsening upwards with grey-green, fine-grained flaggy, micaceous sandstone interbeds.|
18130|Tickalara Metamorphics|22469|6|Mentioned|p18, fig 21||Paleoproterozoic|Halls Creek Province||||||07-NOV-08
18130|Tickalara Metamorphics|22474|5|Briefly described|p20|Orosirian|Orosirian|Age: 1865 Ma.||||||14-NOV-06
18130|Tickalara Metamorphics|22526|3|Fully described|P679, P681, Fig2||Orosirian|Maximum age of unit is 1865 Ma.||||||14-NOV-06
18130|Tickalara Metamorphics|22537|6|Mentioned|34|Proterozoic|Proterozoic|||||||
18130|Tickalara Metamorphics|22547|4|Described|p13||Orosirian|In the Lamboo Complex, Halls Creek Orogen. Age: 1865 Ma. Overlain by Koongie Park Formation.||||||14-NOV-06
18130|Tickalara Metamorphics|22661|6|Mentioned|p 312|||||||||
18130|Tickalara Metamorphics|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Occurs in the central zone of Lamboo Complex.||||||
18130|Tickalara Metamorphics|22754|4|Described|p3|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|22809|6|Mentioned|3|||||||||
18130|Tickalara Metamorphics|23323|4|Described|p454 Fig.2, p457 Fig. 4|Orosirian|Orosirian|Age: 1870-1850Ma.||||||07-FEB-07
18130|Tickalara Metamorphics|23383|6|Mentioned|p9, p5 Tb. 1|||Rocks mapped on ANGELO now recognised as being part of Koongie Park Formation.  Age: c.1865.  Geological Province: Hooper Orogen.||||||25-JAN-05
18130|Tickalara Metamorphics|23599|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Age: c.1865 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23751|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Age: c.1865 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|23897|4|Described|p376, p377 Fig.1|Paleoproterozoic|Paleoproterozoic|Intruded by Sally Malay mafi-ultramafic intrusion.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
18130|Tickalara Metamorphics|23925|5|Briefly described|p220 Fig. 2|Orosirian|Orosirian|Age: c. 1865 Ma.  Geological Province: Halls Creek Orogen.||||||
18130|Tickalara Metamorphics|24173|5|Briefly described|p7, p15|||Possible correlative of Milba Formation and of Halls Creek Group||||||06-APR-05
18130|Tickalara Metamorphics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma.  In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed sedimentary rocks.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
18130|Tickalara Metamorphics|30097|6|Mentioned|Table 23|||See also Tables 24,27 and Fig.54.||||||
18130|Tickalara Metamorphics|30759|6|Mentioned|p16|||Map of East Kimberley Region||||||
18130|Tickalara Metamorphics|30892|6|Mentioned|p96|||Metamorphosed equivalent of Halls Creek Group.||||||14-NOV-06
18130|Tickalara Metamorphics|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18130|Tickalara Metamorphics|31230|6|Mentioned|p182|||||||||
18130|Tickalara Metamorphics|31828|6|Mentioned|p44|||Copper mineralisation||||||
18130|Tickalara Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18130|Tickalara Metamorphics|32660|5|Briefly described|Table 1|||||||||
18130|Tickalara Metamorphics|32728|5|Briefly described|p23|||See also p19.||||||14-NOV-06
18130|Tickalara Metamorphics|33812|5|Briefly described|p2|||Refers Gemuts (1971)||||||
18130|Tickalara Metamorphics|34604|4|Described|p250|||Proterozoic. Metamorphic zoning.||||||
18130|Tickalara Metamorphics|36551|6|Mentioned|p41|||||||||
18130|Tickalara Metamorphics|36885|3|Fully described|p167|||Formerly Halls Creek Metamorphics.||||||14-NOV-06
18130|Tickalara Metamorphics|37462|4|Described|Table 4.I|||Also described p225.||||||14-NOV-06
18130|Tickalara Metamorphics|38460|5|Briefly described|p1567|||||||||
18130|Tickalara Metamorphics|41158|6|Mentioned|p19|||||||||
18130|Tickalara Metamorphics|41465|6|Mentioned|p5|||||||||
18130|Tickalara Metamorphics|41594|6|Mentioned|Fig.15|||||||||
18130|Tickalara Metamorphics|41645|6|Mentioned|p4|||||||||
18130|Tickalara Metamorphics|41976|4|Described|p461|||||||||
18130|Tickalara Metamorphics|41977|5|Briefly described|p473|||||||||
18130|Tickalara Metamorphics|41987|6|Mentioned|p70|||||||||
18130|Tickalara Metamorphics|42326|5|Briefly described|p9|||||||||
18130|Tickalara Metamorphics|42329|5|Briefly described|p5|||See also Fig.2 p6.||||||14-NOV-06
18130|Tickalara Metamorphics|42730|5|Briefly described|p19|||||||||
18130|Tickalara Metamorphics|42757|6|Mentioned|p10|||||||||
18130|Tickalara Metamorphics|42768|6|Mentioned|Fig.6|||||||||
18130|Tickalara Metamorphics|43010|5|Briefly described|p37|||||||||
18130|Tickalara Metamorphics|43853|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|43855|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
18130|Tickalara Metamorphics|43931|5|Briefly described|p20||Orosirian|Age: 1865 Ma. Geological province: Halls Creek Province.||||||14-NOV-06
18130|Tickalara Metamorphics|44155|5|Briefly described|p234-237, p240, p249, p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|U-Pb zircon age from pegmatite.|1854 +/- 6 Ma (Page and Hancock, 1988).|Lamboo Complex||?High-grade equivalent to Halls Creek Group. Faulted against Halls Creek Group. Intruded by Bow River Granite.|Schist, paragneiss, granulite, amphibolite, calc-silicates.|
18130|Tickalara Metamorphics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartz-muscovite-biotite-cordierite hornfels; migmatitic quartz-plagioclase-muscovite-biotite(-sillimanite)-andalusite-cordierite(-chlorite) pelite, and amphibolite. Age: c.1865Ma. In the Lamboo Complex central zone.||||||07-NOV-08
18130|Tickalara Metamorphics|44317|4|Described|Table 1||Proterozoic|||||||
18130|Tickalara Metamorphics|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
18130|Tickalara Metamorphics|44324|14|Not recorded|p.7||Proterozoic|Tb.1, (Proterozoic).||||||
18130|Tickalara Metamorphics|44325|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
18130|Tickalara Metamorphics|44363|5|Briefly described|p.7,8,9,22||Paleoproterozoic|Lower Proterozoic.  In the Lamboo Complex.||||||07-NOV-08
18130|Tickalara Metamorphics|44364|14|Not recorded|map legend|||||||||
18130|Tickalara Metamorphics|44366|14|Not recorded|p.9, Table 1||Proterozoic|||||||
18130|Tickalara Metamorphics|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971). Part of Lamboo Complex. Undifferentiated.||||||14-NOV-06
18130|Tickalara Metamorphics|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
18130|Tickalara Metamorphics|44398|14|Not recorded|map legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44693|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44694|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|44868|5|Briefly described|Map Legend||Proterozoic|||||||
18130|Tickalara Metamorphics|45047|4|Described|p13|||See also pp19-24.  Age.||||||14-NOV-06
18130|Tickalara Metamorphics|45048|4|Described|p10|||See also p11, 23-51. Lower Proterozoic||||||14-NOV-06
18130|Tickalara Metamorphics|45087|6|Mentioned|p186|||Chemical analyses. See also p187, 224, 228, 230, 234.||||||14-NOV-06
18130|Tickalara Metamorphics|45112|6|Mentioned|p47|||||||||
18130|Tickalara Metamorphics|45140|5|Briefly described|p25|||Higher-grade equivalent to the Halls Creek Group. Age given is of the regional metamorphism; maximum age probably 2200 Ma.|1961 +/- 27 Ma (Dow and Gemuts, 1969).|Lamboo Complex.||||
18130|Tickalara Metamorphics|46797|6|Mentioned|p80|||Dates||||||
18130|Tickalara Metamorphics|50437|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Age: 1850-1852 +/- 2Ma (Shrimp).||||||07-NOV-08
18130|Tickalara Metamorphics|60283|5|Briefly described|p24-29|||Halls Creek Orogen. Crops out as relatively flat plains.||||Is intruded by the Panton Intrusion.|Turbidites metamorphosed to granulite facies: quartz-feldspar-muscovite-biotite schists and gneisses.|
18130|Tickalara Metamorphics|60498|5|Briefly described|p1016 Fig.1, p1017 Table 1.|Paleoproterozoic|Paleoproterozoic||||Includes Norton metagabbro.||Amphibolite and granulite facies rocks.|03-JAN-18
18130|Tickalara Metamorphics|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|In the Lambo Complex (Central Zone). Includes: Monkey Yard Tonalite, Fletcher Creek Monzogranite, Dougalls Tonalite.||||||14-NOV-06
18130|Tickalara Metamorphics|60533|6|Mentioned|p592, 593 Fig. 2, 595 Fig. 4, 597|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Age: ca 1865Ma. Overlain unconformably by Red Rock Formation.||||||07-NOV-08
18130|Tickalara Metamorphics|60724|4|Described|p10, p5 Fig. 2|Proterozoic|Proterozoic|Proposed that definition be expanded. Within the Lamboo Complex.||||||
18130|Tickalara Metamorphics|63866|4|Described|p129, p131|||Central Zone, Halls Creek Orogen. Numeric ages are interpreted as the maximum depositional ages for the sedimentary protoliths of this unit. The sedimentary protoliths to these rocks include turbiditic mudstone, siltstone, quartz sandstone, greywacke, chert, carbonates, BIF, mafic volcanics and bimodal sheet-like felsic intrusives. Ages also appear in Bodorkos et al, 1999, 2000a.|Ca. 1865 Ma (Page, OZCHRON)|||(Presumably) overlies the Milba Formation. Intruded by the Rose Bore Granite, Fletcher Creek Monzogranite, Dougall Tonalite and the Dougalls Suite.|Amphibolite and low-pressure granulite facies metasedimentary rocks and meta-igneous rodcks.|
18130|Tickalara Metamorphics|64104|6|Mentioned|p76, p77|Paleoproterozoic|Paleoproterozoic|Possible source of some clasts in Duerdin Group.|||||Schists and calc-silicate rocks.|
18130|Tickalara Metamorphics|64572|6|Mentioned|p802 Fig. 4, p803 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: ~1865Ma. Geological Province: Kimberley Craton.||||||22-DEC-08
18130|Tickalara Metamorphics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated, metamorphosed tonalite and granodiorite, monzogranite, syenogranite; locally migmatitic; Amphibolite; dioritic to gabbroic granulite; migmatitic pelite and psammite, BIF, calc-silicate rock, marble; local volcanic textures, carbonate, hornfels.||||||09-DEC-08
18130|Tickalara Metamorphics|64722|6|Mentioned|p9,10|||Of Halls Creek Orogen. An island arc assemblage accumulated on the southern and southwestern margins of the Kimberley Block. Probably a correlative of the Wangi Basics of the Halls Creek Orogen.||||||
18130|Tickalara Metamorphics|64731|5|Briefly described|pp164-165|Paleoproterozoic|Paleoproterozoic|Central Zone of Halls Creek Orogen. High-grade metamorphism at 1854 +/- 4 Ma (Page & Hancock 1988).||||||12-APR-12
18130|Tickalara Metamorphics|65413|6|Mentioned|p105 Fig.1, p106 Fig.2.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
18130|Tickalara Metamorphics|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Kimberley Province. Hosts Bow River nickel deposit. Correlated with Wangi Basics in Pine Creek Province. Produced in the Bow River Event, ME 6 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1870 Ma.|||||
18130|Tickalara Metamorphics|66845|4|Described|p536 Fig.2, p537, p538, p541|Paleoproterozoic|Paleoproterozoic|Central zone of Lamboo Complex. ?Interrelated with Dougalls suite. Protoliths of this unit were intruded by leucogranite sheets, named Rose Bore Granite and Fletcher Creek Monzogranite ("Eastern Leucocratic Granitoid" of Ogasawara, 1988).|1865-1850 Ma|||intruded by Mabel Downs Tonalite||
18130|Tickalara Metamorphics|66846|6|Mentioned|p549 Fig.2, p552, p554, p556, p558|Orosirian|Orosirian|In the Central Zone of the Lamboo Complex.|||||?mafic volcanics and turbidites.|
18130|Tickalara Metamorphics|67232|5|Briefly described|p30, p34.|Paleoproterozoic|Paleoproterozoic|Central zone of Halls Creek Orogen. Possible correlative of Woolianna Gabbro, Pine Creek Orogen. Low- to high-grade, depleted metabasalt, representing an oceanic island arc/back-arc basin tectonic setting (Sheppard et al. 1999).|c.1865 Ma (Sheppard et al. 1999).|||||
18130|Tickalara Metamorphics|67779|6|Mentioned|p106 Fig.129, p107.|||Arc-related mafic rocks.||||||
18130|Tickalara Metamorphics|68078|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Age is of volcanic and associated sedimentary protoliths.|1865 Ma||||Metasediments and metavolcanics.|
18130|Tickalara Metamorphics|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic||||||Mafic granulite, amphibolite, medium- to high-grade (migmatitic) pelite and psammite, BIF, calc-silicate rock and marble; local pillows and fragmental volcanic textures with interstitial carbonate, and hornfels.|
18130|Tickalara Metamorphics|69003|5|Briefly described|p5, p18-19, p22|||Central zone, Lamboo Province, Halls Creek Orogen.|c.1865 Ma.|||Is intruded by the Savannah intrusion.|Volcanic and associated rocks.|
18130|Tickalara Metamorphics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Rb/Sr age:1920+/-27 Ma. SHRIMP age data from OZCHRON1. Original comment: 'This metamorphic age is based on 17 high-U concordant zircons or zircon rims, and is in good agreement with the conventional zircon data (1851 Ma).'|Metamorphic age: 1852+/-2 Ma U/Pb SHRIMP||Includes Fletcher Creek Granite, Rose Bore Granite and 18 unnamed units.||Mafic extrusive and intrusive meta-igneous rock with interlayered metasedimentary rock; minor metagranitic rock; includes mylonitic rocks: amphibolite, mafic granulite, ultramafic schist, migmatitic pelitic gneiss|04-AUG-15
18130|Tickalara Metamorphics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1733-1920 Ma||||Mylonitized granitic rocks, amphibolite. Mafic granulite, ultramafic schist, amphibolite with interlayered migmatitic, pelitic and psammitic gneiss. Metamudstone, metasiltstone, metasandstone, metacarbonate.|
18130|Tickalara Metamorphics|69422|5|Briefly described|p7:1|||Central Zone, Halls Creek Orogen. Deformed and metamorphosed between 1865 and 1856 Ma and at 1854-1850 Ma.|||||Metasedimentary and meta-igneous rocks.|12-JUL-16
18130|Tickalara Metamorphics|69585|5|Briefly described|p2, p4|Orosirian|Orosirian|Central Lamboo Province. Represents an oceanic island arc.|||||Medium- to high-grade metasedimentary and mafic metavolcanic and metavolcaniclastic rocks.|
18130|Tickalara Metamorphics|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Mafic granulite, amphibolite, medium- to high-grade (migmatitic) pelite and psammite, banded iron-formation, calc-silicate rock, and marble; local pillows and fragmental volcanic textures with intersitial carbonate, and hornfels|
18130|Tickalara Metamorphics|69597|5|Briefly described|p3, p5 |Paleoproterozoic|Paleoproterozoic|Central Lamboo Province. Intruded by sheets of 1850-1845 Ma tonalite.|1865 Ma||||Deformed and metamorphosed mafic volcanic rocks, volcaniclastics, turbidites.|
18130|Tickalara 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 - Central Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1865-1863 Ma (Inferred)||Includes Fletcher Creek Granite, Rose Bore Granite.||Amphibolite; interlayered pelite, psammite, calc-silicate, metamorphosed BIF and marble, mylonite, mafic granulite, metagabbro, ultramafic schist, migmatitic pelitic gneiss, quartz meta-sandstone, -siltstone, -mudstone, metabasalt|
18130|Tickalara Metamorphics|69747|5|Briefly described|p272|Orosirian|Orosirian|Geological province: Halls Creek Orogen. SHRIMP U-Pb dating of detrital zircons yield maximum depositional age of 1867-1864 Ma; crystallisation age of 1857-1855 Ma. Peak metamorphic age from SHRIMP U-Pb dating of monazite and metamorphic zircons of 1845+\-3 Ma and 1845+\-4 Ma respectively. Geochronological dates are derived from Hoatson, 1997; Page et al 1995a.||||||25-JUN-19
18130|Tickalara Metamorphics|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1850-1865 Ma||||Amphibolite containing garnet or clinopyroxene; relict primary layering and gabbroic textures. Mylonitized granitic rocks, mafic granulite, ultramafic schist, migmatitic pelitic gneis,metamudstone, metasiltstone, metasandstone and metacarbonate.|
18130|Tickalara Metamorphics|70731|5|Briefly described|p268-273,277-278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. [Misspelt Ticklara Metamorphics on p278]. Associated with oceanic arc development of the central Lamboo Province at c. 1865 Ma outboard of the NAC. Deformed and metamorphosed to amphibolite and granulite facies at 1865-1856 Ma, and 1850-1845 Ma during the Hooper Orogeny (Blake et al., 2000a; Bodorkos et al., 1999; Bodorkos and Reddy, 2004; Page et al., 2001). Underwent rifting c. 1845-1840 Ma, resulting in formation of the Koongie Park Formation. Median density: 2850 kg/m3.||||||
18130|Tickalara Metamorphics|70812|4|Described|p3, p6, p8-p9, p12, p14|Orosirian|Orosirian|Central Zone of the Halls Creek Orogen, Lamboo Province. Metamorphosed at high temperature, low pressure amphibolite to granulite facies at 1865-1856 and 1850-1845 Ma during the Hooper and Halls Creek orogenies. Mineralisation is described. See also p18, p20, p24-p25, p27-p28, p31, p43.|c. 1865 Ma|||Intruded by the Dougalls Suite and the McIntosh Suite.|Mafic volcanic and volcaniclastic rocks, granulite facies rocks and migmatites.|
18130|Tickalara Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
18130|Tickalara Metamorphics|70851|4|Described|p3-p5, p7, p11-p12|Paleoproterozoic|Paleoproterozoic|Central Zone, Lamboo Province. Deformed and metamorphosed to amphibolite and granulite facies  during the Hooper Orogeny. Intruded by the c. 1856 Ma Panton Intrusion. Rock properties are provided and geophysical response is discussed. See also p17-p19, p23, p28-p29, p35.|c. 1865 Ma|||Intruded by the Panton Intrusion.|Sedimentary, mafic volcanic and volcaniclastic rocks.|
18130|Tickalara Metamorphics|71113|4|Described|p95-100,102-103,108-112|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Intruded and metamorphosed by Dougalls Suite at 1850 Ma in an island arc (Sheppard et al., 2001) or convergent continental margin setting (Sheppard et al., 1997). Underwent regional HTLP metamorphism at 1845+\-4 Ma (Bodorkos et al., 1999; Oliver and Barr, 1997; Oliver et al., 1999; Thornett, 1986). Exposed units metamorphosed to granulite-facies, in faulted contact with non-metamorphosed Sally Downs Supersuite. Underwent rifting at 1845-1840 Ma at the end of Hooper Orogeny. Protolith sedimentary and igneous rocks may have been formed in either (1) an oceanic island arc setting above E-dipping subduction zone outboard of Kimberley Craton, or in (2) an ensialic marginal basin located closer to the margin of Kimberley Craton above a W-dipping subduction (Sheppard et al., 1999b). Geochemical analysis of depleted and enriched metabasalts indicate depleted light REEs signatures of both oceanic island arc/back-arc and MORB affinities (Sheppard et al., 199b). Numerical models with an active continental margin setup show the development of an ensialic marginal basin for deposition of the protoliths to the Tickalara Metamorphics and successfully replicate the geological evolution of the Lamboo Province.|1865 Ma|||Overlain by Koongie Park Formation. Intruded by Dougalls Suite. In fault contact with Sally Downs Supersuite.|Mafic volcanic and turbiditic sedimentary rocks.|
18130|Tickalara Metamorphics|71140|5|Briefly described|p95-103, 108-111|Orosirian|Orosirian|Oldest rocks in the Central Zone, Lamboo Province, Halls Creek Orogen. Intruded and metamorphosed c.1850 Ma. Rifting occurred 1845-1840 Ma.|c.1865 Ma.|||Is intruded by Dougalls Suite. Is faulted against Sally Downs Supersuite.|Low- to high-grade (granulite facies) metamorphosed turbiditic sedimentary and mafic submarine volcanic and volcaniclastic protoliths.|
18130|Tickalara 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 (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, 100k_interpgeol_lut.csv and geochron files.|1865-1850 Ma (inferred)|Unit of Dougalls Suite.|Includes Fletcher Creek Granite, Rose Bore Granite, Corkwood Tonalite, Dead Finish Tonalite, Dougalls Tonalite, Monkey Yard Tonalite.||Amphibolite; interlayered pelite, psammite, calc-silicate, metamorphosed BIF and marble, mylonite, mafic granulite, metagabbro, ultramafic schist, migmatitic pelitic gneiss, quartz meta-sandstone, -siltstone, -mudstone, metabasalt|
18130|Tickalara Metamorphics|71281|5|Briefly described|p422|||Central Zone, Lamboo Province.||||Is intruded by Sally Downs Supersuite.|Dominated by a medium- to high-grade succession of metaturbidites, hosting mafic metavolcanic and volcaniclastic rocks with oceanic island-arc geochemical affinities.|
18130|Tickalara Metamorphics|71397|5|Briefly described|p4-6,14,44,47|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Deposited in either an oceanic islandarc/ back-arc setting or an ensialic basin margin outboard of Kimberley Craton during east-directed subduction (Sheppard et al., 1999b; Griffin et al., 2000a). Evidence of deformation includes layer-parallel foliation and isoclinal folding at c. 1863-1850 Ma, and subsequent folding and medium to high T, LP metamorphism at c. 1845 Ma. Bodorkos et al. (1999) provided a maximum depositional age of c. 1865 Ma for sedimentary protoliths.|c. 1865-1850 Ma||||Middle to upper amphibolite to granulite facies mafic volcanic and intrusive rocks with interlayered metasedimentary and volcaniclastic rocks; MORB-like composition in lower part.|
18130|Tickalara Metamorphics|71873|5|Briefly described|p426-427,430,432,434-435,439-445|Orosirian|Orosirian|Geological province: Lamboo Province. Dominant in the Central Zone and comprises mafic volcanic (pillowed) and intrusive rocks with interlayered metasedimentary rocks at upper amphibolite to granulite facies. Comprises clasts of metamorphic and graphitic rocks, indicating a continental source. Metamorphosed to greenschist facies; folded and then intruded by Kevins Dam Suite. Magmatic-textured detrital zircons yield maximum depositional ages of 1869+\-4 and 1869+\-6 Ma. Contains recrystallized magmatic grains and metamorphic rims dated at 1862+\-6, 1864+\-15 and 1838+\-13 Ma. the c. 1860 Ma ages may have formed shortly after sediment deposition and are likely to be detrital metamorphic zircons. The younger age may represent metamorphic zircon formed in-situ within the sediment.|c. 1870 Ma||Includes Rose Bore granite.|||
18130|Tickalara Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Mafic extrusive and intrusive meta-igneous rock with interlayered metasedimentary rock; minor metagranitic rock.|
18130|Tickalara Metamorphics|72437|5|Briefly described|p5-p7, p14, p24, p41-44|Palaeoproterozoic|Palaeoproterozoic|Protoliths are intruded by leucogranite sheets. Two analyses are provided, one of the migmatite and one of the metaturbidite. Intruded by a zoned alkaline plug referred to as the Copperhead Albitite 'Carbonatite' Complex.|c. 1870 Ma||||Mafic amphibolite, granulite, migmatite and metaturbidite.|
18130|Tickalara Metamorphics|73089|5|Briefly described|p32-33, p37|Orosirian|Orosirian|Lamboo Province, Central Zone. Dominantly Paleoproterozoic detritus in metasedimentary rocks. Mafic volcanic rocks have geochemical characteristics that can be interpreted in terms of a back-arc/ensialic rift setting, or an oceanic arc.|c. 1875-1855 Ma||||Includes metasedimentary units and mafic volcanic rocks.|
18130|Tickalara Metamorphics|73427|6|Mentioned|p3|||North Australian Craton, Lamboo Province. Basalts may have formed during convergent margin processes.||||||
18186|Timperley Shale|22496|3|Fully described|p11||Neoproterozoic|Of the Albert Edward Group.  Inferred to overlie the Douri Sandstone.  Geological Province: Wolfe Basin.||||||16-AUG-04
18186|Timperley Shale|22547|6|Mentioned|p28||Neoproterozoic III|Of the Albert Edward Group.||||||14-NOV-06
18186|Timperley Shale|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
18186|Timperley Shale|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Overlying unit Nyuless Sandstone. Underlying unit Douri Sandstone. Geological Province: Wolfe Basin. Max. thickness: 1000 m.||||||
18186|Timperley Shale|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
18186|Timperley Shale|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Albert Edward Group.||||||
18186|Timperley Shale|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Albert Edward Group.  Recessive, thinly bedded, dark greenish grey siltstone, shale and mudstone.  Geological Province: Wolfe Basin. Max Thickness: >1000m.||||||06-APR-05
18186|Timperley Shale|29813|4|Described|Table 2|||||||||
18186|Timperley Shale|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18186|Timperley Shale|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18186|Timperley Shale|32109|6|Mentioned|Table 1|||Precambrian||||||
18186|Timperley Shale|32172|6|Mentioned|p10|||Dated 666 +/- 43my (Bofinger,1967).||||||
18186|Timperley Shale|32660|5|Briefly described|Table 6|||||||||
18186|Timperley Shale|32728|6|Mentioned|Table 7|||See also Fig.16||||||
18186|Timperley Shale|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18186|Timperley Shale|36551|6|Mentioned|Table 12|||||||||
18186|Timperley Shale|36888|4|Described|p214|||||||||
18186|Timperley Shale|36898|5|Briefly described|Table II|||||||||
18186|Timperley Shale|37462|6|Mentioned|p294|||||||||
18186|Timperley Shale|37927|6|Mentioned|p511|||||||||
18186|Timperley Shale|38157|6|Mentioned|Table X|||||||||
18186|Timperley Shale|39210|5|Briefly described|p49|||Age.||||||05-SEP-18
18186|Timperley Shale|41429|6|Mentioned|p248|||||||||
18186|Timperley Shale|43299|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
18186|Timperley Shale|43303|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
18186|Timperley Shale|44140|5|Briefly described|p301 fig 4-7, p302 Tb. 4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 1265 m thick.||Albert Edward Group||Overlies Boonall Dolomite conformably. Overlain by Nyuless Sandstone conformably.|Massive grey and green shale and siltstone; interbedded dolomite near base; conformable sequence.|08-MAR-18
18186|Timperley Shale|44317|14|Not recorded|Table 3,p.7||Adelaidean|||||||
18186|Timperley Shale|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
18186|Timperley Shale|44324|14|Not recorded|p.10||Adelaidean|Tb.2, (Adelaidean). Of Albert Edward Group.||||||
18186|Timperley Shale|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
18186|Timperley Shale|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
18186|Timperley Shale|45047|2|Defined|p96|late Adelaidean|late Adelaidean|See p36.||||||18-MAY-15
18186|Timperley Shale|45140|3|Fully described|p13, p59-60, Appx.p38|||Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Mount Timperley. [No type section details]. 100m to over 1000m thick. No fossils known. NB: The definition in Appx.p38 has confused the overlying and underlying units.||Albert Edward Group.||Conformably overlies Boonall Dolomite or Elvire Formation. Is overlain conformably by Nyuless Sandstone or Flat Rock Formation. See Comments.|Maroon micaceous shale and siltstone with minor thin interbeds of lithic arenite.|
18186|Timperley Shale|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
18186|Timperley Shale|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Alber Edward Group. Geological Province: Wolfe Creek Basin. Grey-green mudstone and siltstone; minor sandstone.||||||
18186|Timperley Shale|63458|5|Briefly described|p873 Fig.2, p884, p897 Fig.19.|Ediacaran|Ediacaran|||Unit in Albert Edward Group.||Conformably overlies Boonall Dolomite.|Mudstone.|12-JUN-15
18186|Timperley Shale|64104|6|Mentioned|p62 fig.1. |Neoproterozoic|Neoproterozoic|||Unit in Albert Edward Group.||||
18186|Timperley Shale|67484|6|Mentioned|p294, p295 Fig.2|Ediacaran|Ediacaran|East Kimberley.||Of the Albert Edward Group.||Overlain by the Nyuless Sandstone. Underlain by the Boonall Dolomite.||
18186|Timperley Shale|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Boonall Dolomite. Is overlain by Nyuless Sandstone.||
18186|Timperley Shale|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Albert Edward Group.||||
18186|Timperley Shale|68244|4|Described|p660,p666-667|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region.||Unit of Albert Edward Group.||Overlain by Nyuless Sandstone. Underlain by Boonall Dolomite.|Marine shales and sandstones|21-JUN-19
18186|Timperley Shale|68473|6|Mentioned|p531, p533|||||Albert Edward Group||The lower part is equivalent to the Yurabi Formation. Underlies the Flat Rock Formation.||
18186|Timperley Shale|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Albert Edward Group|Includes two unnamed members.||Grey-green mudstone and siltstone; minor thinly bedded lithic sandstone, quartz sandstone, calcareous sandstone and interbedded dolomite.|04-AUG-15
18186|Timperley Shale|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv.|||||Grey-green mudstone and siltstone; minor sandstone. Quartz sandstone, calcareous sandstone and siltstone. Massive to thin bedded to laminated micaceous shale and siltstone with minor thinly bedded lithic sandstone.|
18186|Timperley Shale|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.|||Massive to thin bedded to laminated, micaceous, grey and green shale and siltstone; minor thinly bedded lithic sandstone, quartz sandstone, calcareous sandstone, siltstone and interbedded dolomite near base|
18186|Timperley Shale|70154|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Albert Edward Group|||siltstone/mudstone|05-SEP-18
18186|Timperley Shale|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 massive to thin bedded to laminated micaceous grey and green shale and siltstone with minor thinly bedded lithic sandstone, and interbedded dolomite near base|
18186|Timperley Shale|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||Albert Edward Group||Overlies the Boonall Dolomite, underlies the Nyuless Sandstone.||
18259|Togobinna Formation|29845|6|Mentioned|Table 69|||||||||
18269|Tollu Group|22561|5|Briefly described|p15|||Rb-Sr whole rock age of 1064+/-23 Ma||||||
18269|Tollu Group|23716|5|Briefly described|p30|Stenian|Stenian|Age: 1078+/-5 Ma.||||||
18269|Tollu Group|24197|5|Briefly described|p97|||Of the Bentley Supergroup. Includes the Smoke Hill volcanics. Geological province: Musgrave Complex.||||||07-FEB-11
18269|Tollu Group|24301|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Age: 1078+/-5Ma (Glickson et al, 1996).  Geological Province: Musgrave Block||||||05-AUG-08
18269|Tollu Group|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|See also Tollu Volcanics and Tollu Formation Volcanics. Of Bentley Supergroup. Geological Province: Musgrave Block.||||||
18269|Tollu Group|30386|4|Described|p6|||See also P7. Proterozoic age.||||||
18269|Tollu Group|30388|6|Mentioned|p7|||Equivalent ? to Pussy Cat Group||||||
18269|Tollu Group|30389|6|Mentioned|p15|||||||||
18269|Tollu Group|30390|4|Described|p54|||||||||
18269|Tollu Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
18269|Tollu Group|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18269|Tollu Group|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18269|Tollu Group|31970|6|Mentioned|p15|||||||||
18269|Tollu Group|32727|5|Briefly described|p10|||Stratigraphy. Dates||||||
18269|Tollu Group|33478|6|Mentioned|p451|||||||||
18269|Tollu Group|35308|6|Mentioned|p451|||||||||
18269|Tollu Group|36551|6|Mentioned|Table 31|||||||||
18269|Tollu Group|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18269|Tollu Group|36886|4|Described|p196|||||||||
18269|Tollu Group|37299|6|Mentioned|Fig.1|||||||||
18269|Tollu Group|37707|6|Mentioned|p24|||||||||
18269|Tollu Group|42940|5|Briefly described|p1|||||||||
18269|Tollu Group|43052|6|Mentioned|p162|||||||||
18269|Tollu Group|43609|6|Mentioned|p13|||||||||
18269|Tollu Group|43688|5|Briefly described|p174|||||||||
18269|Tollu Group|43692|6|Mentioned|p128|||Approx. 1060 Ma: extrusion age||||||
18269|Tollu Group|43693|5|Briefly described|p107|||||||||
18269|Tollu Group|43696|6|Mentioned|p41|||||||||
18269|Tollu Group|43697|6|Mentioned|p27|||||||||
18269|Tollu Group|44109|3|Fully described|p117|Mesoproterozoic|Mesoproterozoic|Of the Bentley Supergroup. Includes the Hogarth Formation, Smoke Hill Felsic Volcanics, Mummawarrawarra Basalt and MacDougall Formation. Volcanic rocks. Overlain by the Townsend Quartzite. Age: 1078+/-5Ma. See also p9, p80.||||||
18269|Tollu Group|44139|5|Briefly described|p284, Table 3-16|Neoproterozoic|Mesoproterozoic|Of Bentley Supergroup. ~500m. Basalt, minor rhyolite. May be equivalent to Pussy Cat Group. Rb-Sr whole rock isochron of acid volcanics: 1060+/-140 Ma (Compston & Nesbitt, 1967).|| ||||10-SEP-12
18269|Tollu Group|45149|5|Briefly described|p19|||||||||
18269|Tollu Group|50607|6|Mentioned|p1.1, 3.2|||Geological Province: Musgrave Block. Of the Bentley Supergroup.||||||
18269|Tollu Group|61154|5|Briefly described|p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Bentley Supergp. See also Tollu Volcanics (relationship unclear?).  Includes MacDougall Bluff Fm., Mummawarrawarra Basalt, Smoke Hill Felsic Volcanics and Hogarth Fm. Age: 1078+/-5Ma.  Geol.Prov: Musgrave Block. Correlated with Tjauwata Group.||||||03-AUG-05
18269|Tollu Group|61339|6|Mentioned|Map legend|||Of the Bentley Supergroup. Includes Hogarth Formation, Smoke Hill Felsic Volcanics, Mummawarrawarra Basalt and Macdougall Formation. See also in Solid Geology Sketch Map and Summary chart.||||||21-SEP-05
18269|Tollu Group|61340|6|Mentioned|Summary chart/Map legend|||||||||
18269|Tollu Group|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Volcanics. Geological Province: Musgrave Province.||||||
18269|Tollu Group|61864|6|Mentioned|p18 fig 4|||Volcanics.||||||
18269|Tollu Group|62453|6|Mentioned|p15|||Of the Bentley Supergroup. Age: 1078 +/- 5Ma.||||||
18269|Tollu Group|62989|5|Briefly described|p39, p40|||Of the Bentley Supergroup. Includes Mummawarrawarra Basalt,  Smoke Hill Volcanics and Hogarth Formation.  In W.A.||||||25-JAN-07
18269|Tollu Group|63465|5|Briefly described|p554|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup in the west Musgrave Block. Age: 1078+/-5Ma. Coeval with Giles Complex Intrusion.||||||11-JUL-13
18269|Tollu Group|63562|6|Mentioned|p341||||1075 +/- 5 Ma (Close et al., 2005).|||Correlated with Tjauwata Group.||
18269|Tollu Group|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Bentley Supergroup. Includes; Smoke Hill Volcanics, Mummawarrawarra Basalt and Macdougall Formation.||||||
18269|Tollu Group|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
18269|Tollu Group|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup. Rhyolite, dacite, ignimbrite, basalt, volcaniclastic sedimentary rock, sandstone, and conglomerate.||||||09-DEC-08
18269|Tollu Group|64722|5|Briefly described|Fig. 2 p3-6, p17|Stenian|Stenian|Has equivalents Tjauwata Group and Bentley Supergroup. Age from (member) Smoke Hill Volcanics. Smithies et al. (2008) give a preliminary age of 1026+/-26 and divide this unit into the older Kunamanara Group and a younger re-defined Tollu Group.|1078 +/- 5 Ma.|||||11-APR-12
18269|Tollu Group|64725|6|Mentioned|p64.|||||Unit in Bentley Supergroup.||||
18269|Tollu Group|64745|5|Briefly described|p376, p373 Fig. 3, p374 Tab. 1|Stenian|Stenian|Includes Hogarth Formation (uppermost unit), and paper implies also includes Puntitjata Rhyolite. Bimodal volcanics, including rhyolite. Age: in range of ca. 1.08-1.04Ga. Geol. Prov: Musgrave Province. See Tollu Group.||||||01-SEP-09
18269|Tollu Group|65135|1|Redefined|p1, p6 Fig.4, p16|Stenian|Stenian|Of the Bentley Supergroup. Originally defined by Daniels (1971) as basal sandstones, pebbly sandstones and conglomerates of the MacDougall Formation, overlain by Mummawarrawarra Basalt, which is in turn overlain by Smoke Hill Volcanics and Hogarth Formation. Original Tollu Formation redefined and subdivided in this paper into the Kunmarnara Group (lower original Tollu Group) and the redefined Tollu Group.  A dacite from the (redefined) Tollu Group is dated at 1026 +/- 26 Ma. Redefined Tollu Group contains Smoke Hill Volcanics and Hogarth Formation. Felsic rocks of Tollu Formation are possibly more than 50 myr older than unconformably underlying Kunmarnara Group. ~1075-1025 Ma.||||||16-JAN-15
18269|Tollu Group|65256|5|Briefly described|p9, p14|Tonian|Stenian|Of the Bentley Supergroup; includes MacDougall Formation, Mummawarrawarra Basalt, Smoke Hill Felsic Volcanics, Hogarth Formation. Thought to be a lateral equivalent of the Pussy Cat Group; correlative of the Tjauwata Group.||||||
18269|Tollu Group|65693|5|Briefly described|p3, p8, pp11-12 Figs. 8-10.|||Outcrops immediately to the south of Blackstone Range. Has different geochemistry (higher La/Nb and Zr content) from Alcurra Suite; details in text.|1026 +/- 26 Ma.|||||22-APR-20
18269|Tollu Group|65833|5|Briefly described|p1, p6 Fig.4, p16|Stenian|Stenian|Of Bentley Supergroup. Defined by Daniels (1974) as including basal MacDougall Formation, Mummawarrawarra Basalt, Smoke Hill Volcanics and Hogarth Formation. The first two units have been reassigned in this paper to the (underlying) Kunmarnara Group, because feeder dykes to volcanic units in the Tollu Group cut through these mafic-ultramafic intrusions. A dacite constituent is aged 1026 +/- 26 Ma.||||||
18269|Tollu Group|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bentley Supergroup, Bentley Basin. Map implies age between c.1075 and c. 1067 Ma. Trachytic, dacitic, rhyolitic volcanic rocks with associated subvolcanic granophyre sills; acicular hornblende needles to 3cm; locally plagioclase porphyritic.||||||
18269|Tollu Group|65906|5|Briefly described|p3, p8, p10, p19-23|Neoproterzoic|Mesoproterozoic|Part of the Bentley Supergroup. Bimodal volcanics and interlayered sedimentary rocks. Includes the Hogarth Formation. Includes rhyolite. Age: ~1075-1060 Ma. Overlies Giles Complex.||||||
18269|Tollu Group|66256|6|Mentioned|p16|||Eruption of felsic lavas.|c. 1075 to 1026 Ma.|||||11-JAN-17
18269|Tollu Group|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes Smoke Hill Volcanics and Hogarth Formation.||Rhyolitic to andesitic volcanic rocks; porphyritic rhyolite and lesser dacite.|
18269|Tollu Group|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Consists of Smoke Hill Volcanics in this map area.||Unit in Bentley Supergroup.|Includes Smoke Hill Volcanics.|||
18269|Tollu Group|67128|4|Described|p1, p5 Fig.3, p7, p11, p15, p25, p30-33|||See also p28 Fig.17. Musgrave Province. Redefined by Smithies et al. (2009) into a basal rift succession (Kunmarnara Group) and a Tollu Group of Smoke Hill Volcanics and Hogarth Formation. Associated with felsic dykes, sheets and plutons to 12 km diameter in the Giles Event. The age appears twice in the text as c.1030 Ma.|c.1075 to 1026 Ma.|Bentley Supergroup.|Smoke Hill Volcanics, Hogarth Formation.|Overlies Blackstone intrusion. Is intruded by the Warakurna Supersuite.|Felsic lavas.|
18269|Tollu Group|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes Smoke Hill Volcanics.|||
18269|Tollu Group|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Bentley Supergroup.|Includes Smoke Hill Volcanics and Hogarth Formation.|||
18269|Tollu Group|67375|1|Redefined|p7, p38 Table 1, pp40-41, p220, p299-331|Mesoproterozoic|Mesoproterozoic|Redefined. The lower two units (MacDougall Formation and Mummawarrawarra Basalt) now comprise the Kunmarnara Group. May be laterally equivalent to Pussy Cat Group. Outcrop is almost entirely restricted to the east-trending Blackstone syncline, Blackstone Sub-basin. Hosts copper-gold vein style mineralization north of the Cavenagh Range.|1073 +/- 7 - 1026 +/- 26 Ma (Coleman et al.2010b).|Unit in Bentley Supergroup.|Included basal MacDougall Formation, Mummawarrawarra Basalt, Smoke Hill Volcanics and Hogarth Formation. Redefined to include just the last two units; the first two comprise the Kunmarnara Group.|Unconformably overlies Kunmarnara Group.|Basal sandstones, pebbly sandstones and conglomerate; overlain by amygdaloidal basalts; these overlain by felsic lavas, then basic to intermediate volcanic rocks.|
18269|Tollu Group|67553|4|Described|p8,11,17,20-21,35,38,40,42-43,59|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Blackstone Sub-basin, Bentley Sub-basin. Underwent N-S directed compression, coeval with uplifting of Kathleen Ignimbrite block. Present-day distribution is restricted to the central part of the Blackstone Sub-Basin immediately to the south of the Blackstone Range. See also p64-65,85-86,89.|1073-1068 Ma|Unit of Bentley Supergroup.|Includes Hogarth Formation and Smoke Hill Volcanics.|Underlain by Kunmarnara Group.||
18269|Tollu Group|68100|5|Briefly described|p5|||Redefined by Smithies et al. (2009), to exclude MacDougall Formation and Mummawarrawarra Basalt (now both Kunmarnara Group).||Bentley Supergroup|Includes Smoke Hill Volcanics, Hogarth Formation,||Felsic and mafic volcanics.|19-JAN-17
18269|Tollu Group|68995|6|Mentioned|p3 Fig.1, p4 Fig.2, p24, p64|Stenian|Stenian|Blackstone Sub-basin.|c. 1075-1071 Ma|Bentley Supergroup|Smoke Hill Volcanics|||
18269|Tollu Group|68996|5|Briefly described|p5, 7, 32-33, 39, 41, 43, 47,67|Mesoproterozoic|Mesoproterozoic|Depositional age range ~1073-1068 Ma. See also pp50, 52, 55-57, 62,63,64,65.|1073 +/- 7 Ma (SHRIMP)|Bentley Supergroup|Includes Smoke Hill Volcanics, Hogarth Formation||Granites, rhyolites and andesitic volcanic rocks. Density values range from 2.68-2.99g/cm^3.|
18269|Tollu Group|69003|6|Mentioned|p37|Mesoproterozoic|Mesoproterozoic|Blackstone Sub-basin, west Musgrave Province.||||||
18269|Tollu Group|69009|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Only shown on Interpreted Bedrock Geology diagram.||Of the Bentley Supergroup.|||Comprises rhyolitic to andesitic volcanic rocks.|28-MAY-15
18269|Tollu Group|69091|4|Described|p52 Fig.4.1, p54 Fig.4.2, see comments|Mesoproterozoic||Remnant of a presumably larger Blackstone Sub-basin (Smithies et al., 2009b). See also p74, p131 Fig.6.1, p133, p134 Fig.6.2, p144.|Hogarth Formation date 1068 +/- 7 Ma (GSWA, 2011)|Bentley Supergroup|Smoke Hill Volcanics, Hogarth Formation.|Overlies Giles Suite.||07-OCT-14
18269|Tollu Group|69153|5|Briefly described|geologyp_lut.csv; Rocks.csv; more|||Data also located in WAMIN.csv and SITE_LITHOLOGY.csv||Bentley Supergroup|Hogarth Formation, Smoke Hill Volcanics||Sample description: igneous mafic volcanic; basalt; mineralized quartz vein in mafic volcanics|
18269|Tollu Group|69436|5|Briefly described|p21:14|||Daniels (1974) included the MacDougall Formation and Mummawarrawarra Basalt in this Group. Now they are reassigned to the Kunmarnara Group. Blackstone Sub-basin [Bentley Basin].||Bentley Supergroup.|Smoke Hill Volcanics, Hogarth Formation.|Unconformably overlies the (redefined) Kunmarnara Group.||12-JUL-16
18269|Tollu Group|69655|5|Briefly described|p3, p5-p6, p33-p35, p77-p78|Stenian|Stenian|Blackstone Sub-basin.|c. 1090-1040 Ma|Bentley Supergroup||Intruded by the Alcurra Dolerite suite.||
18269|Tollu Group|69729|6|Mentioned|p66 Fig.1, p68, p70, p80|||Blackstone Sub-basin.|||Smoke Hill Volcanics, Hogarth Formation.|||
18269|Tollu Group|70634|6|Mentioned|500k_geologyp08_lut,csv|Mesoproterozoic|Mesoproterozoic|||Bentley Supergroup|Includes Smoke Hill Volcanics, Hogarth Formation, Smoke Hill Volcanics (2)||Undivided; rhyolite, dacite, ignimbrite, basalt, volcaniclastic sedimentary rock, sandstone, and conglomerate.|
18269|Tollu Group|70793|5|Briefly 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, 500k_interpgeol_lut.csv.||Unit of Bentley Supergroup.|Includes Hogarth Formation, Smoke Hill Volcanics.|Underlain unconformably by Giles Suite intrusions.||
18269|Tollu Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup||||
18269|Tollu Group|70831|5|Briefly described|p3, p5|||Blackstone Sub-basin.||Bentley Supergroup||||
18269|Tollu Group|70839|6|Mentioned|p326|||Geological province: Musgrave Province. Of Blackstone Sub-basin, Bentley Basin.||||||
18269|Tollu Group|71088|6|Mentioned|p5|||Musgrave Province.||Bentley Supergroup||||
18269|Tollu Group|71170|5|Briefly described|p5-p6|||Blackstone Sub-basin.||Bentley Supergroup||||
18269|Tollu Group|71210|5|Briefly described|p4-p5, p9, p21, p27, p51, p79, p113|||Blackstone Sub-basin.||Bentley Supergroup|Includes the Smoke Hill Volcanics and the Hogarth Formation.|||
18269|Tollu Group|71211|6|Mentioned|p6 fig 1.3, p7 fig 1.4, p24 fig 2.1|||See also  p84 fig 3.1, p136 fig 4.1 , p233.||Bentley Supergroup|Includes the Hogarth Formation, Smoke Hill Volcanics.|||
18269|Tollu 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). 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.||Unit of Bentley Supergroup.|Includes Hogarth Formation.|Underlain unconformably by Giles Suite intrusions.|Rhyolitic and basaltic volcanic rocks; conglomerate and sandstone|
18269|Tollu Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|Max age 1073+/-7 Ma, min age 1026+/-26 Ma.|Bentley Supergroup|||Rhyolitic and basaltic volcanic rocks; conglomerate and sandstone.|
18269|Tollu Group|72094|6|Mentioned|p3 Fig 2|Mesoproterozoic|Mesoproterozoic|Blackstone Sub-basin, Bentley Basin.||||||
18269|Tollu Group|72443|6|Mentioned|p737, p744, p750|||Blackstone Sub-basin.|||Includes the Smoke Hill Volcanics and the Hogarth Formation.|||
18269|Tollu Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Blackstone Sub-basin.||Bentley Supergroup||||
18275|Tolmer Group|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, dolomite.||||||
18275|Tolmer Group|9538|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, dolomite, siltstone.   Age: >900Ma.||||||
18275|Tolmer Group|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||||||
18275|Tolmer Group|14019|5|Briefly described|p2 Fig. 1|||On the FERGUSSON RIVER  and PINE CREEK  sheets.  Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|22479|5|Briefly described|fig1p2|||Placed in Litchfied Province.||||||11-DEC-06
18275|Tolmer Group|22809|5|Briefly described|1|||Underlain by Burrell Creek Formation.||||||18-NOV-11
18275|Tolmer Group|22810|5|Briefly described|Table3 P7, P18||Proterozoic|Minimum age: 1200 Ma; maximum age 1780+/-80 Ma.||||||11-DEC-06
18275|Tolmer Group|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, dolomite.||||||19-OCT-05
18275|Tolmer Group|23216|6|Mentioned|Fig3p5,33||Mesoproterozoic|||||||
18275|Tolmer Group|23714|4|Described|p36|Proterozoic|Proterozoic|See also page 7 Table 1. Geological Province: Litchfield Province. Max. thickness 1800 m.||||||
18275|Tolmer Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Sandstone, dolomite, siltstone.  Geological Province: Litchfield Province (Pine Creek Orogen).  See also p6 Fig. 5.||||||07-NOV-08
18275|Tolmer Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|24260|6|Mentioned|p1015 Fig.3|||Geological Province: Pine Creek Inlier||||||
18275|Tolmer Group|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|||||||
18275|Tolmer Group|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlies the Pine Creek Geosyncline.  Unconformably overlain by the Limbunya Group. Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|24442|5|Briefly described|p30, p43|||Includes: Depot Creek, Stray Creek Sandstones and Hinde Dolostone.  Marine sandstones mainly.  Overlies the Finniss River Group. See also p50 Fig. 1.||||||
18275|Tolmer Group|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
18275|Tolmer Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|32660|4|Described|Table 6|||||||||
18275|Tolmer Group|32700|4|Described|p15|||Refers Randal (1962). Much now Bullita and Auvergne Groups.||||||11-DEC-06
18275|Tolmer Group|32728|6|Mentioned|p16|||||||||
18275|Tolmer Group|32873|6|Mentioned|Fig.1|||||||||
18275|Tolmer Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|33377|6|Mentioned|Fig.|||||||||
18275|Tolmer Group|33729|6|Mentioned|p81|||Fauna.||||||
18275|Tolmer Group|34287|6|Mentioned|p41|||||||||
18275|Tolmer Group|35465|6|Mentioned|Fig.1|||Geology of Pine Creek Geosyncline||||||
18275|Tolmer Group|35495|6|Mentioned|p350|||||||||
18275|Tolmer Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18275|Tolmer Group|37462|4|Described|Table 4.VI|||||||||
18275|Tolmer Group|37579|5|Briefly described|Regional setting map legend|Adelaidean|Adelaidean|Sandstone, dolomite, siltstone. Probably  Adelaidean.||||||10-OCT-05
18275|Tolmer Group|38157|6|Mentioned|p284|||||||||
18275|Tolmer Group|38243|6|Mentioned|p355|||||||||
18275|Tolmer Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18275|Tolmer Group|39069|6|Mentioned|Fig.5|||||||||
18275|Tolmer Group|39210|5|Briefly described|p49|||||||||
18275|Tolmer Group|39320|6|Mentioned|Fig.1|||||||||
18275|Tolmer Group|39563|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
18275|Tolmer Group|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|39801|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Prob.Late Proterozoic. Sandstone, dolomite, siltstone.||||||05-OCT-05
18275|Tolmer Group|39803|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40105|6|Mentioned|p316|||See also Fig.3||||||
18275|Tolmer Group|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, dolomite, siltstone.||||||18-OCT-05
18275|Tolmer Group|40223|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, dolomite, siltstone.||||||19-OCT-05
18275|Tolmer Group|40495|6|Mentioned|p13|||||||||
18275|Tolmer Group|40765|6|Mentioned|Fig.3|||||||||
18275|Tolmer Group|40808|6|Mentioned|p17|||||||||
18275|Tolmer Group|40809|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40823|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|40852|6|Mentioned|p25|||||||||
18275|Tolmer Group|40957|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18275|Tolmer Group|41125|6|Mentioned|Fig.6|||||||||
18275|Tolmer Group|41304|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
18275|Tolmer Group|41305|6|Mentioned|Fig.4|||||||||
18275|Tolmer Group|41407|6|Mentioned|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|41645|6|Mentioned|Fig.4|||||||||
18275|Tolmer Group|41646|6|Mentioned|Map legend|Mesoproterozoic||Sandstone, siltstone, dolomite.||||||17-OCT-05
18275|Tolmer Group|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Hinde Dolomite, Stray Creek Sandstone and Depot Creek Sandstone. Sandstone, siltstone, dolomite.||||||07-OCT-05
18275|Tolmer Group|41661|3|Fully described|p18|||Mention p23 and Fig.5.||||||11-DEC-06
18275|Tolmer Group|41878|6|Mentioned|p34|||||||||
18275|Tolmer Group|41980|6|Mentioned|p585|||||||||
18275|Tolmer Group|42012|4|Described|p13|||||||||
18275|Tolmer Group|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
18275|Tolmer Group|43140|5|Briefly described|p4||Mesoproterozoic|||||||
18275|Tolmer Group|43187|5|Briefly described|p7|||||||||
18275|Tolmer Group|43624|6|Mentioned|Table 1, p9,37|Adelaidean|Carpentarian|||||||
18275|Tolmer Group|43832|5|Briefly described|29,Table7 p27, 97||Mesoproterozoic|"Middle Proterozoic Platform Cover". Underlain by Finniss River Group.||||||
18275|Tolmer Group|44113|5|Briefly described|p240|Adelaidean|Adelaidean|Geological Province: Daly River Basin.||||||11-DEC-06
18275|Tolmer Group|44314|2|Defined|p.6-7,map|||(D52-4). DARWIN Sheet.||||||11-DEC-06
18275|Tolmer Group|44315|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
18275|Tolmer Group|45022|3|Fully described|p.91.||Adelaidean|On many pages.||||||11-DEC-06
18275|Tolmer Group|45064|5|Briefly described|p14|||||||||
18275|Tolmer Group|45102|6|Mentioned|p49|||||||||
18275|Tolmer Group|45112|3|Fully described|p24|||p24-29.||||||11-DEC-06
18275|Tolmer Group|46163|14|Not recorded|p.168,170,171|||||||||
18275|Tolmer Group|46658|6|Mentioned|p560|||||||||
18275|Tolmer Group|46675|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Waterbag Creek Formation, Hinde Dolomite, and Buldiva Sandstone. Sandstone, dolomite, siltstone. Unconformably overlain by the Daly River Group; unconformably overlies the Finniss River Group.   Geological Province: Pine Creek Geosyncline.||||||29-NOV-04
18275|Tolmer Group|46676|14|Not recorded|p.6||Neoproterozoic|U.Proterozoic; includes Buldiva Sandstone, Hind Dolomite & Waterbag Creek Formation.||||||
18275|Tolmer Group|47049|6|Mentioned|p237|||||||||
18275|Tolmer Group|48867|14|Not recorded|p.7|||map. Katherine-Darwin area.||||||
18275|Tolmer Group|48942|6|Mentioned|p43|||Refers Randal (1962) & Walpole et al. (1968).||||||
18275|Tolmer Group|50623|6|Mentioned|p259 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18275|Tolmer Group|60526|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Sandstone, dolomite, siltstone.||||||
18275|Tolmer Group|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Buldiva Sandstone.||||||
18275|Tolmer Group|60685|5|Briefly described|p4 Fig. 3|Proterozoic|Proterozoic|Correlated with Birrindudu Group. Geological Province: Birrindudu Basin.||||||
18275|Tolmer Group|61389|5|Briefly described|Map Legend|||||||||
18275|Tolmer Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Neoproterozoic|Paleoproterozoic|Sandstone, dolostone, siltstone. Thickness: 1000m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
18275|Tolmer Group|63261|5|Briefly described|p17, p24|||Correlative of Birrindudu Group. Unconformably overlies the western Pine Creek Orogen.||||||07-FEB-11
18275|Tolmer Group|63866|5|Briefly described|p106-p107, p117, p123|||Litchfield Province, Pine Creek Orogen.||||Unconformably overlies the Wangi Basics and Zamu Dolerite. Equivalent to the Katherine River Gorup.||
18275|Tolmer Group|64698|5|Briefly described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma.  Includes Depot Creek Sandstone, Stray Creek Sandstone, Waterbag Creek Formation, Hinde Dolostone (here misspelt as Hindrance Dolostone).||||||07-JAN-09
18275|Tolmer Group|64722|6|Mentioned|p10|||Of western Pine Creek Orogen. Possible correlative of the Birrindudu Group.||||||12-APR-12
18275|Tolmer Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Birrindudu Basin unit deposited during the Calvert Event (~1730-1690 Ma)||||||
18275|Tolmer Group|64730|6|Mentioned|p127|Paleoproterozoic|Paleoproterozoic|in the Litchfield Province. Possible correlate of Katherine River Group, McArthur Basin.||||||
18275|Tolmer Group|64956|6|Mentioned|p62|Mesoproterozoic|Mesproterozoic|Overlies Soldiers Creek Granite.||||||07-FEB-11
18275|Tolmer Group|65232|5|Briefly described|p52, p6 Fig. 5, p5 Fig. 4, p78|Palaeoproterozoic|Palaeoproterozoic|With Katherine River Group are correlatives of Birrindudu, Hatches Creek, Tomkinson Creek, and Tawallah Groups. Sedimentary rocks: sandstone, dolomite, siltstone. Geol. Prov: western Pine Creek Orogen.||||||09-FEB-10
18275|Tolmer Group|65339|5|Briefly described|p4, p5 Fig.4, p14, p16.|||Unconformably overlies Pine Creek Orogen rocks.|||||Sandstone, conglomerate, greywacke.|
18275|Tolmer Group|65342|5|Briefly described|pp10-11.|||Birrindudu Basin.|||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|Is unconformably overlain by Limbunya Group.|Mostly coarse siliciclastic sedimentary rocks.|
18275|Tolmer Group|67167|5|Briefly described|Map legend.|||Areas with different magnetic responses are indicated.|||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|||18-NOV-11
18275|Tolmer Group|67186|5|Briefly described|Map legend.||||||Includes Depot Creek and Stray Creek Sandstones and Hinde Dolostone.|||23-NOV-11
18275|Tolmer Group|67269|5|Briefly described|p20-21 Fig.19|Statherian|Orosirian|Birrindudu Basin.|1825-1700 Ma.||Hinde Dolostone.|||
18275|Tolmer Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p32|||Pine Creek area.|~1760 Ma deposition.||||Sandstone, dolomite, siltstone.|
18275|Tolmer Group|67355|6|Mentioned|p7 Fig.5, p14, p26, p27 Fig.18, p68||Paleoproterozoic||||Depot Creek Sandstone.|Unconformably overlies the Whites Formation and Coomalie Dolostone.||25-JAN-17
18275|Tolmer Group|67479|6|Mentioned|p2 Tb.1, p15, p58||||||Includes the Depot Creek Sandstone.|||
18275|Tolmer Group|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Western Pine Creek Orogen. Correlative of Katherine River Group to the east.|||||Sandstone, dolostone, siltstone.|
18275|Tolmer Group|67779|5|Briefly described|p6 Fig.5, p32.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Formerly Buldiva Quartzite of Hossfeld (1937). Correlated with Katherine River Group by Noakes (1949) who later (1956) revoked the correlation.|||Includes Depot Creek and Stray Creek Sandstones; Hinde Dolostone, and Waterbag Creek Formation.|||21-MAY-18
18275|Tolmer Group|68280|6|Mentioned|p26 fig 24|||Birrindudu Basin.|||Includes Hinde Dolostone|||
18275|Tolmer Group|68575|5|Briefly described|p125|||Western Pine Creek Orogen. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Kombolgie Subgroup; Westmoreland Conglomerate).|||Depot Creek Sandstone.|||
18275|Tolmer Group|68733|6|Mentioned|p186||||||Depot Creek Sandstone.|||06-DEC-17
18275|Tolmer Group|69383|5|Briefly described|p31|Mesoproterozoic|Mesoproterozoic|||||Overlies Burrell Creek Formation.||
18275|Tolmer Group|69417|5|Briefly described|p2:5-6|Statherian|Statherian|Northern Birrindudu Basin. Represents part of a single, large un-named superbasin linked at depth beneath overlying basins.||||||12-JUL-16
18275|Tolmer Group|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
18275|Tolmer Group|69420|5|Briefly described|p5:14, 54, 64|||Birrindudu Basin. Associated with Au mineralisation in the underlying Coomalie Dolostone.|||Depot Creek Sandstone.|Unconformably overlies Coomalie Dolostone.||12-JUL-16
18275|Tolmer Group|69432|4|Described|p17:1-3, 5-6, 12-13|Paleoproterozoic|Paleoproterozoic|Noakes (1956), for a succession of sandstone, dolostone and shale unconformably overlying the Pine Creek Orogen and unconformably overlain by the Daly Basin succession. Birrindudu Basin. A likely correlative of the Katherine River Group.  1600-1800m thick. Unfolded: horizontal to gently dipping. Age poorly constrained: lacks reliable chronostratigraphic control. SHRIMP U-Pb detrital zircon maximum deposition age of 1837 +/- 15 Ma by Claoue-Long et al. (2001).|<1837 Ma.||Depot Creek, Stray Creek, Sandstones; Hinde Dolostone.|Unconformably overlies Inverway Metamorphics. Is overlain unconformably by Limbunya Group.||12-JUL-16
18275|Tolmer Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p49|Statherian|Statherian|1600-1800m thick.|||Includes Depot Creek Sandstone, Stray Creek Sandstone, Hinde Dolostone, Waterbag Creek Formation|Unconformably overlain by Limbunya Group|Sandstone, dolostone and shale with minor conglomerate and siltstone packages. Parts of the succession are glauconitic, stromatolitic or dolomitic.|
18275|Tolmer Group|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Includes Waterbag Creek Formation; Hinde Dolostone; Stray Creek, Depot Creek Sandstones.|Is overlain by Uniya Formation.||01-MAR-18
18275|Tolmer Group|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.|||Includes Hinde Dolostone, Stray Creek Sandstone, Depot Creek Sandstone.|Overlain by Limbunya Group. Underlain by Inverway Metamorphics. Equivalent to Birrindudu Group.||
18275|Tolmer Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Tawallah Group (central/southern McArthur Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
18344|Toodyay Quartzite|24410|6|Mentioned|p27|||Silica rock used as dimension stone in the building industry. Also referred to as Toodyay Stone in the industry.||||||
18344|Toodyay Quartzite|37577|6|Mentioned|p56|||||||||
18394|Toolonga Calcilutite|6876|6|Mentioned|p100 Fig.5.|Late Cretaceous|Late Cretaceous|||||||
18394|Toolonga Calcilutite|12471|6|Mentioned|p475 Fig.2. |Late Cretaceous|Late Cretaceous|||||Overlies Gearle Siltstone. Is overlain by Cardabia Calcarenite.||
18394|Toolonga Calcilutite|12729|6|Mentioned|p9 Fig.6, p17.|Late Cretaceous|Late Cretaceous|Widespread, deposited in a low-energy, inner- to middle-shelf, marine environment.||||Conformably overlain by the Korojon Calcarenite, unconformably overlain by the Miria Formation and Tertiary rocks, disconformably overlies the Winning Group.|Limestone and shale. Massive, fossiliferous calcilutite and calcisiltite.|
18394|Toolonga Calcilutite|13255|6|Mentioned|p369|Late Cretaceous|Late Cretaceous|Roebuck Basin.||||Overlies Nelson Rocks Formation. Is overlain by Miria Marl.||
18394|Toolonga Calcilutite|13615|3|Fully described|p4-p5, p6-p8, p19-p20|Maastrichtian|Coniacian|Peedamullah Shelf. Up to 310m thick. Spores/Pollen Zone and Dinoflagellate zones provided. Type section occurs at Murchison House Station; 27deg36'00"S 114deg13'40"E. Contains Santonian-Campanian and locally Maastrichtian Fauna-mostly foraminifers. Deposited in a low energy marine shelf environment. See also p35, p56, p58, p72, p81, p101 App. 3, p118, Plates 2, 3.||||Disconformably overlies the Gearle Siltstone. Disconformably overlain by the Cardabia Group and Trealla Limestone.|Fossiliferous, pale calcilutite and calcisiltite.|12-FEB-19
18394|Toolonga Calcilutite|14228|5|Briefly described|p5 Fig.2, p9, p16|Cretaceous|Cretaceous|Gascoyne Platform.Up to 300 m thick.||||Grades up and laterally into Korojon Calcarenite. Overlies (disconformably) Winning Group. Overlain by Miria Formation.|Fossiliferous calcilutite and calcisiltite.|
18394|Toolonga Calcilutite|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
18394|Toolonga Calcilutite|23311|5|Briefly described|map legend|Late Cretaceous|Late Cretaceous|||||||
18394|Toolonga Calcilutite|23312|5|Briefly described|map legend|Maastrichtian|Turonian|||||||
18394|Toolonga Calcilutite|23379|5|Briefly described|p159, 160, 167 Fig.2||Campanian|of Barrow Sub-basin (Carnarvon Basin).||||||
18394|Toolonga Calcilutite|23403|4|Described|p9|Cretaceous|Cretaceous|||||||24-NOV-09
18394|Toolonga Calcilutite|23433|5|Briefly described|p111|Late Cretaceous|Late Cretaceous|||||||
18394|Toolonga Calcilutite|23520|5|Briefly described|p6 Fig. 4|Late Cretaceous|Late Cretaceous|Geological Province: Abrolhos Sub-basin.  See also p12.||||||
18394|Toolonga Calcilutite|23572|4|Described|p5, 12|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin. Underlying Unit: Winning Group (disconformable). Overlying Unit: Miria Formation. Max. thickness: 273m.||||||
18394|Toolonga Calcilutite|23620|5|Briefly described|p4 Fig. 4|Cretaceous|Cretaceous|Predominantly calcareous pelagic deposits.||||||01-SEP-08
18394|Toolonga Calcilutite|23726|5|Briefly described|p95|Late Cretaceous|Late Cretaceous|Overlying unit Miria Formation. Underlying unit Alinga Formation. Geological Province: Carnarvon Basin.||||||
18394|Toolonga Calcilutite|23815|4|Described|p298|Campanian|Santonian|Formerly known as the "Toolonga Chalk". Geological Province: Carnarvon Basin. Overlying unit: Korojon Calcarenite (conformable). Underlying units: Alinga Formation and Gearle Siltstone (disconformable). Max. thickness: 273 m. Fossiliferous.||||||
18394|Toolonga Calcilutite|23915|5|Briefly described|p520|Campanian|Coniacian|Overlies; Gearle Siltstone (disc).  Type section detailed in text.  See also p518 Table 1. Geological Province: Southern Carnarvon Basin.||||||
18394|Toolonga Calcilutite|23935|4|Described|p11 Fig.7|Campanian|Coniacian|Unconfromably overlies Winning Group. White and yellow/grey fossiliferous calcilutite. Thickness: 65 m. Geological Province: Southern Carnarvon Basin.||||||
18394|Toolonga Calcilutite|23976|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
18394|Toolonga Calcilutite|23977|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
18394|Toolonga Calcilutite|23978|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
18394|Toolonga Calcilutite|24059|5|Briefly described|p132|Late Cretaceous|Late Cretaceous|Geological Province: Barrow Sub-basin.||||||
18394|Toolonga Calcilutite|24060|5|Briefly described|p160|Santonian|Santonian|Geological Province: Dampier Sub-basin.||||||
18394|Toolonga Calcilutite|24084|5|Briefly described|p146 Fig.2|Late Cretaceous|Late Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
18394|Toolonga Calcilutite|24094|5|Briefly described|p268, p275|Santonian|Santonian|Overlain by Korojon Calcarenite.  Replaces Toolonga Chalk? Geological Province: Carnarvon Basin||||||16-MAR-05
18394|Toolonga Calcilutite|24160|5|Briefly described|p36, 38|Late Cretaceous|Late Cretaceous|||||Grades laterally into Alinga Formation. Conformably overlies Gearle Siltstone and Haycock Marl.||
18394|Toolonga Calcilutite|24205|6|Mentioned|p250 Fig. 6|||||||||
18394|Toolonga Calcilutite|24331|5|Briefly described|p475 Fig.2|Late Cretaceous|Late Cretaceous|Unconformably overlies Gearle Siltstone. Unconformably overlain by Cardabia Calcarenite. Marine. Geological Province: Barrow Sub-basin.||||||
18394|Toolonga Calcilutite|24351|5|Briefly described|Plate 3, Plate 4 (in pocket)|Late Cretaceous|Late Cretaceous|Geological Province: Exmouth Plateau, Exmouth Sub-basin, Gascoyne Platform/Sub-basin. Log Wittecarra-1||||||13-DEC-07
18394|Toolonga Calcilutite|24410|5|Briefly described|p134 Fig. 79|Phanerozoic|Phanerozoic|||||||24-NOV-09
18394|Toolonga Calcilutite|24551|6|Mentioned|p632|||||||||
18394|Toolonga Calcilutite|29381|4|Described|p67|||||||||
18394|Toolonga Calcilutite|29721|6|Mentioned|Table 102|||||||||
18394|Toolonga Calcilutite|30016|6|Mentioned|p92|||Cretaceous||||||
18394|Toolonga Calcilutite|30265|6|Mentioned|p89|||Small flow of gas and oil encountered in North Rankin No.!.||||||
18394|Toolonga Calcilutite|30304|4|Described|p53|||||||||
18394|Toolonga Calcilutite|30335|6|Mentioned|p17|||||||||
18394|Toolonga Calcilutite|30365|6|Mentioned|Fig.8|||||||||
18394|Toolonga Calcilutite|30875|6|Mentioned|p10|||See also P13. Upper Cretaceous (Senonian).||||||
18394|Toolonga Calcilutite|31083|6|Mentioned|Fig. 2|||||||||
18394|Toolonga Calcilutite|31396|6|Mentioned|p1184|||||||||
18394|Toolonga Calcilutite|31561|5|Briefly described|p34|||See also P6. Late Cretaceous||||||
18394|Toolonga Calcilutite|31604|5|Briefly described|p6|||Santorian to Maestrichtian||||||
18394|Toolonga Calcilutite|32024|6|Mentioned|p16|||||||||
18394|Toolonga Calcilutite|32025|6|Mentioned|p988|||Oil at North Rankin No. 1||||||
18394|Toolonga Calcilutite|32166|5|Briefly described|p159|||||||||
18394|Toolonga Calcilutite|32391|6|Mentioned|p10|||||||||
18394|Toolonga Calcilutite|32648|6|Mentioned|p32|||U.Cret.||||||
18394|Toolonga Calcilutite|32711|6|Mentioned|p446|||See also Fig.3||||||
18394|Toolonga Calcilutite|32714|6|Mentioned|Fig.7|||U.Cret.||||||
18394|Toolonga Calcilutite|32715|6|Mentioned|p1182|||Oil||||||
18394|Toolonga Calcilutite|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
18394|Toolonga Calcilutite|33165|6|Mentioned|Chart|||Correlation chart only||||||
18394|Toolonga Calcilutite|33386|6|Mentioned|Fig.7|||||||||
18394|Toolonga Calcilutite|33450|6|Mentioned|Fig.3|||See P11.||||||
18394|Toolonga Calcilutite|33453|6|Mentioned|p72|||Strat.||||||
18394|Toolonga Calcilutite|33813|6|Mentioned|p7|||See also Table 2||||||
18394|Toolonga Calcilutite|34231|6|Mentioned|p66|||||||||
18394|Toolonga Calcilutite|34363|6|Mentioned|p56|||See also P57. Senonian.||||||
18394|Toolonga Calcilutite|34721|6|Mentioned|p286|||||||||
18394|Toolonga Calcilutite|34727|6|Mentioned|p68|||||||||
18394|Toolonga Calcilutite|34730|6|Mentioned|p80|||||||||
18394|Toolonga Calcilutite|34838|6|Mentioned|p3|||||||||
18394|Toolonga Calcilutite|34846|6|Mentioned|Fig.3|||||||||
18394|Toolonga Calcilutite|35057|6|Mentioned|p301|||||||||
18394|Toolonga Calcilutite|35059|6|Mentioned|p205|||||||||
18394|Toolonga Calcilutite|35105|6|Mentioned|Fig.5|||||||||
18394|Toolonga Calcilutite|35144|6|Mentioned|Fig.3|||||||||
18394|Toolonga Calcilutite|35275|6|Mentioned|Fig.5.|||||||||
18394|Toolonga Calcilutite|35282|6|Mentioned|Fig.2|||||||||
18394|Toolonga Calcilutite|35983|6|Mentioned|p148|||||||||
18394|Toolonga Calcilutite|36093|6|Mentioned|Fig.2|||||||||
18394|Toolonga Calcilutite|36257|6|Mentioned|Table 2.1|||||||||
18394|Toolonga Calcilutite|36305|6|Mentioned|p353|||||||||
18394|Toolonga Calcilutite|36890|3|Fully described|p298|||Formerly Toolonga Chalk.||||||11-APR-08
18394|Toolonga Calcilutite|37016|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
18394|Toolonga Calcilutite|37302|6|Mentioned|p74|||||||||
18394|Toolonga Calcilutite|37320|6|Mentioned|p237|||||||||
18394|Toolonga Calcilutite|37360|6|Mentioned|Fig.3|||||||||
18394|Toolonga Calcilutite|37577|6|Mentioned|p75|||||||||
18394|Toolonga Calcilutite|37689|6|Mentioned|p25|||On schematic section.||||||
18394|Toolonga Calcilutite|38444|6|Mentioned|p301|||||||||
18394|Toolonga Calcilutite|38485|4|Described|p16|||||||||
18394|Toolonga Calcilutite|38998|4|Described|p18|||||||||
18394|Toolonga Calcilutite|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
18394|Toolonga Calcilutite|39427|4|Described|Table 1|||||||||
18394|Toolonga Calcilutite|39486|6|Mentioned|Fig.2|||||||||
18394|Toolonga Calcilutite|40340|5|Briefly described|p15|||||||||
18394|Toolonga Calcilutite|40341|6|Mentioned|Map legend|Campanian|Santonian|||||||
18394|Toolonga Calcilutite|40342|6|Mentioned|Map legend|Campanian|Santonian|Santonian - Campanian||||||
18394|Toolonga Calcilutite|40343|5|Briefly described|p12|||||||||
18394|Toolonga Calcilutite|40617|6|Mentioned|p15|||||||||
18394|Toolonga Calcilutite|40800|6|Mentioned|p4|||||||||
18394|Toolonga Calcilutite|40801|6|Mentioned|p42|||||||||
18394|Toolonga Calcilutite|40992|6|Mentioned|Fig.8|||||||||
18394|Toolonga Calcilutite|41170|6|Mentioned|p155|||See also P157||||||
18394|Toolonga Calcilutite|41172|6|Mentioned|p129|||||||||
18394|Toolonga Calcilutite|41271|3|Fully described|p157|||Mention P18||||||
18394|Toolonga Calcilutite|41280|4|Described|p143|||||||||
18394|Toolonga Calcilutite|41436|6|Mentioned|Fig.6|||||||||
18394|Toolonga Calcilutite|41438|6|Mentioned|p109|||||||||
18394|Toolonga Calcilutite|41439|6|Mentioned|p123|||||||||
18394|Toolonga Calcilutite|41440|4|Described|p139|||||||||
18394|Toolonga Calcilutite|41441|6|Mentioned|Fig.6|||||||||
18394|Toolonga Calcilutite|41443|6|Mentioned|Fig.3 P160|||Actually shown as just Toolonga Calc.||||||
18394|Toolonga Calcilutite|41444|6|Mentioned|Fig.4|||||||||
18394|Toolonga Calcilutite|41446|6|Mentioned|p203|||||||||
18394|Toolonga Calcilutite|41447|6|Mentioned|Fig.3 P226|||Mistakenly recorded as Toolonga Calcarenite 1988-Feb 1992.||||||
18394|Toolonga Calcilutite|41709|6|Mentioned|Fig.7|||See also Fig.5||||||
18394|Toolonga Calcilutite|41712|6|Mentioned|Fig.8 P278|||Actually shows only Toolonga Calc in figure.||||||
18394|Toolonga Calcilutite|41729|6|Mentioned|Fig.2|||||||||
18394|Toolonga Calcilutite|41732|6|Mentioned|Fig.3|||||||||
18394|Toolonga Calcilutite|42075|5|Briefly described|Fig.4 P245|||Figure actually only shows Toolonga Cal.||||||
18394|Toolonga Calcilutite|42116|5|Briefly described|p10, p18, Fig.1 p6|Cretaceous||||||||
18394|Toolonga Calcilutite|42123|4|Described|Fig.8 P34|||||||||
18394|Toolonga Calcilutite|42393|3|Fully described|p101|Campanian|Santonian|Type section designated in 1958 & clarified 1987. Age: early Santonian to early Campanian.||||||11-APR-08
18394|Toolonga Calcilutite|42395|6|Mentioned|Fig.22 P85|||||||||
18394|Toolonga Calcilutite|42463|6|Mentioned|Fig.2 P169|||||||||
18394|Toolonga Calcilutite|42473|6|Mentioned|p75|||||||||
18394|Toolonga Calcilutite|42995|3|Fully described|p34|||||||||
18394|Toolonga Calcilutite|43173|5|Briefly described|13||Late Cretaceous|||||||
18394|Toolonga Calcilutite|43564|6|Mentioned|Fig.2,p446|Campanian|Santonian|||||||
18394|Toolonga Calcilutite|43598|6|Mentioned|p814|Campanian|Santonian|(Early Campanian)||||||
18394|Toolonga Calcilutite|43712|5|Briefly described|p12||Turonian|||||||
18394|Toolonga Calcilutite|43722|5|Briefly described|p11||Turonian|||||||
18394|Toolonga Calcilutite|43724|5|Briefly described|p30||Turonian|||||||
18394|Toolonga Calcilutite|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
18394|Toolonga Calcilutite|43827|5|Briefly described|p194|||||||||
18394|Toolonga Calcilutite|44143|4|Described|p430 Table 4-19; p449 Figure 4-108, p450|Cretaceous|Cretaceous|>200m thick; limestone (calcilutite); marine. Bedout Sub-basin.||||||24-NOV-17
18394|Toolonga Calcilutite|44159|5|Briefly described|Table p.37||Late Cretaceous|||||||
18394|Toolonga Calcilutite|44532|14|Not recorded|p.9,10, map|||(G50-5).||||||
18394|Toolonga Calcilutite|44533|5|Briefly described|map legend||Late Cretaceous|Upper Cretaceous.||||||
18394|Toolonga Calcilutite|44995|14|Not recorded|p.6-198||Late Cretaceous|U.Cretaceous forams.||||||
18394|Toolonga Calcilutite|45015|5|Briefly described|map legend|Late Cretaceous|Late Cretaceous|||||||01-JUN-06
18394|Toolonga Calcilutite|45142|6|Mentioned|Fig.4|||||||||
18394|Toolonga Calcilutite|46808|6|Mentioned|Table 2|||||||||
18394|Toolonga Calcilutite|46883|6|Mentioned|p213|||||||||
18394|Toolonga Calcilutite|46950|6|Mentioned|Fig.15|||||||||
18394|Toolonga Calcilutite|48609|14|Not recorded|p.11,12, Pl.3|||||||||
18394|Toolonga Calcilutite|48610|14|Not recorded|Pl.1|||(F50-13).||||||
18394|Toolonga Calcilutite|48628|14|Not recorded|p.4,5|||||||||
18394|Toolonga Calcilutite|48831|14|Not recorded|p.33|||||||||
18394|Toolonga Calcilutite|48848|14|Not recorded|p.65|||||||||
18394|Toolonga Calcilutite|48861|2|Defined|p6|Campanian|Santonian|p.5, Pl.1. Lowest unit of Cardabia Group. Santonian-Campanian.||||||11-FEB-19
18394|Toolonga Calcilutite|48925|6|Mentioned|p7|||Upper Cretaceous - Santonian age. Fauna.P11||||||
18394|Toolonga Calcilutite|49942|4|Described|p4 Fig.3|Late Cretaceous|Late Cretaceous|Overlies Haycok Marl (unconformably) and Winning Group (disconformably) where Haycock Marl absent. Overlain by Korojon Calcarenite (conformable) and Miria Marl (unconformable). Fossiliferous calcilutite and calcsiltite. Geol. Province: Gascoyne Platform.||||||
18394|Toolonga Calcilutite|50085|5|Briefly described|p23 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
18394|Toolonga Calcilutite|60384|5|Briefly described|p244, p243 Fig 2a|Late Cretaceous|Late Cretaceous|Perth and Carnarvon Basins. Overlies Haycock Marl.||||Overlies Haycock Marl and disconformably overlies Winning Group in places|Calcilutite and calcisiltite|
18394|Toolonga Calcilutite|60386|6|Mentioned|p289||Cretaceous|||||||
18394|Toolonga Calcilutite|60709|5|Briefly described|p830|Maastrichtian|Campanian|Calcareous claystone. Geol.Prov: Southern Carnarvon Platform. See also the misspelt Tooloonga Calcilutite.||||||
18394|Toolonga Calcilutite|61023|5|Briefly described|p27 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||11-APR-08
18394|Toolonga Calcilutite|61155|5|Briefly described|p15|||Interfingers with Miria Formation. Age is pre-Cainozoic. Geological Province: Carnarvon Basin/onshore||||||
18394|Toolonga Calcilutite|61811|4|Described|p3 Fig.2, p9 Table 3, p11, pp13-16, p65.|Campanian|Santonian|Northern Perth Basin. About 25 m thick. Reference section (Lynch 1991) is described. Type section details in Appendix 1. Formerly the Toolonga Chalk and Second Gully Shale of Clarke and Teichert (1948); combined as Toolonga Calcilutite by Johnstone et al. (1958). Contains abundant forams, used to correlate this unit with Gingin Chalk.||||Overlies Haycock Marl, and (disconformably) Alinga Formation.|Friable greenish marly calcilutite with thin indurated horizons; thin basal layer of small phosphatic nodules, and thin laterally extensive layer of flint nodules 7 m above base of unit; white chalk with >50% Inoceramus fragments; glauconitic chalk.|
18394|Toolonga Calcilutite|61958|5|Briefly described|Map sheet 1|Late Cretaceous|Late Cretaceous|||||||
18394|Toolonga Calcilutite|62734|5|Briefly described|p1362 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
18394|Toolonga Calcilutite|62837|5|Briefly described|Stratigraphic columns|Campanian|Santonian|Age: >85-75Ma. Geological Province: Northern Carnarvon Basin and Roebuck Basin.||||||01-MAR-10
18394|Toolonga Calcilutite|63068|5|Briefly described|p44 Fig. 2|Campanian|Coniacian|Geological Province: Carnarvon Basin.||||||
18394|Toolonga Calcilutite|63950|5|Briefly described|p336 Fig. 4|Campanian|Santonian|Geological Province: northern Carnarvon Basin.||||||27-MAY-08
18394|Toolonga Calcilutite|64580|4|Described|map legend|Pleistocene|Late Cretaceous|Undivided; limestone ranging from calcilutite to calcirudite, in part algal bound; minor siliciclastic sandstone.||||||09-DEC-08
18394|Toolonga Calcilutite|64635|5|Briefly described|p4 Fig.3, p7 |Campanian|Coniacian|||||||
18394|Toolonga Calcilutite|64977|6|Mentioned|p493 Fig.3.|Late Cretaceous|Late Cretaceous|Thevenard Island area.||||Unconformably overlies Gearle Siltstone. Is unconformably overlain by Cardabia Calcarenite.||
18394|Toolonga Calcilutite|66193|5|Briefly described|p569 Fig.2|Late Cretaceous|Late Cretaceous|in offshore Canning Basin, overlies Nelson Rocks Formation, underlies the Miria Marl||||||
18394|Toolonga Calcilutite|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes light grey marl.|
18394|Toolonga Calcilutite|67200|5|Briefly described|p8 fig 6, p18 table 1|Cretaceous|Cretaceous|Thermal conductivity of 1.45 W/mK. See also p46, p50, p53, app 2 tbl 1.||||Unconformably overlies Alinga Formation, Gearle Siltstone, Haycock Marl, unconformably overlain by Miria Formation|Crudely bedded calcilutite, limestone and marl.|
18394|Toolonga Calcilutite|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||||||
18394|Toolonga Calcilutite|67368|6|Mentioned|p209 Fig.4.|Late Cretaceous|Late Cretaceous|||||Overlies Haycock Marl. Is overlain by Withnell Formation.||
18394|Toolonga Calcilutite|67369|6|Mentioned|p251.|||The top of this unit was used as a seismic marker for interpreting the Pluto Field data.||||||
18394|Toolonga Calcilutite|67784|6|Mentioned|p30 Fig.7||Cenomanian|Carnarvon Basin.||||||
18394|Toolonga Calcilutite|67970|5|Briefly described|p4, p10, p25 Fig.4.|Campanian|Santonian|Exmouth Plateau.|||||Mid-outer shelf marl and chalk.|
18394|Toolonga Calcilutite|68206|6|Mentioned|p30|Aptian|Aptian|Carnarvon Basin.||||||
18394|Toolonga Calcilutite|69182|6|Mentioned|Ch3 p3, Ch3 p8, Ch3 p12|||Carnarvon Basin. Misspelt as the Toolonga "Calcilurinte" in Ch3 p69. See also Ch3 p23-p26, Ch3 p30, Ch3 p35, Ch3 p37, Ch3 p65-p66, Ch3 p69, Ch3 p71.||||Overlain by the Miria Formation and the Korojon Calcarenite. Disconformably overlain by the Cardabia Calcarenite.||
18394|Toolonga Calcilutite|69297|5|Briefly described|p247, p249, p337|Turonian|Turonian|Gascoyne Sub-basin of the Southern Carnarvon Basin and Canning, Roebuck Basins.||||Overlies the Gearle Siltstone and the Haycock Marl. Unconformably overlies the Nelson Rocks Formation. Overlain by the Korojon Calcarenite or the Miria Formation.|Calcilutite.|
18394|Toolonga Calcilutite|69558|5|Briefly described|p27, p95, p96, p97 fig 151, p98|Campanian|Santonian|Well exposed in the valley of the Murchison river (~100km to S) and is the oldest rock exposed in Shark Bay. Outcrop characteristics discussed. See also p157 fig 240, p226, p235, p235 fig 379, p252.||||Overlain by the Giralia Calcarenite.|White chalk and greenish-white calcareous mudstone.|26-MAY-21
18394|Toolonga Calcilutite|69692|6|Mentioned|p4|Late Cretaceous|Late Cretaceous|Northern Carnarvon Basin.||||Overlies Upper Gearle Siltstone. Is overlain by Withnell Formation.||
18394|Toolonga Calcilutite|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4|Campanian|Santonian|Roebuck Basin and offshore Canning Basin.||||Overlies Nelson Rocks Formation. Is overlain by Miria Formation.||01-MAY-19
18394|Toolonga Calcilutite|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Campanian|Turonian|See also Regional: Fig.6. Northern Carnarvon Basin.||||Overlies Haycock Marl and Gearly Siltstone. Is overlain by Withnell Formation.||
18394|Toolonga Calcilutite|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Southern Carnarvon Basin.||||||
18394|Toolonga Calcilutite|70906|5|Briefly described|p757-758|Late Cretaceous|Late Cretaceous|Gorgon Platform.||||Overlies Gearle Siltstone. Is overlain by Withnell Formation.||
18394|Toolonga Calcilutite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, crystalline dolostone/dolomite, calcilutite|
18394|Toolonga Calcilutite|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Plateau.||||Overlies Gearle Siltstone. Is overlain by Korojon Calcarenite.||
18405|Toondi Formation|22663|5|Briefly described|S97-1 and 2 p3|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
18405|Toondi Formation|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
18405|Toondi Formation|41751|2|Defined|p2|Cenomanian|Albian|||||||
18405|Toondi Formation|42315|6|Mentioned|p2|Cenomanian|Albian|||||||
18405|Toondi Formation|42545|3|Fully described|p16|Cenomanian|Albian|Variation on Toondi Formation, WA.||||||
18405|Toondi Formation|43498|6|Mentioned|8|Santonian|Neocomian|||||||
18405|Toondi Formation|44133|5|Briefly described|p134|Cenomanian|Albian|Disconformably overlies Madura Formation. Disconformably overlain by Nurina Formation. Originally included in Madura Formation.||||||
18405|Toondi Formation|44145|4|Described|p549 fig 4-190, p553-4, p551, p554|Cenomanian|Albian|Eucla Basin. Type section in Transcontinental Railway 1 bore, Madura. Age from palynomorphs. Previously included in Madura Formation.||||Disconformably overlies Madura Formation.|Siltstone, claystone and shale. Minor sandstone; commonly pyritic.|
18405|Toondi Formation|61197|5|Briefly described|p473, p475, p478 Fig.4|Middle Cretaceous|Middle Cretaceous|Eucla Basin. Low-energy marine deposits. 0-60m thick.|||||Silt, clay/shale; minor sand; pyritic.|
18405|Toondi Formation|61630|6|Mentioned|p555 Fig. 3|Turonian|Albian|Geological Province: Eyre Sub-basin. Marine.||||||07-APR-09
18405|Toondi Formation|63124|5|Briefly described|p72|||Marine deposits. Geological Province: Bight Basin. Equivalent to Eumeralla Formation.||||||
18405|Toondi Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Aptian|Bight Basin.||||||
18405|Toondi Formation|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9, p60|Turonian|Albian|Eyre Sub-basin.||||Equivalent to the Ceduna and Platypus Formations.|Shale.|
18445|Torrens Formation|13222|6|Mentioned|p229 Fig.2.|||Appears in the diagram simply as Torrens due to lack of space, and so the rank of this unit is not specified. Probably an informal name; the database lists a Torrens Group in SA which would thus have precedence.||Unit in Kinmore Group.||||
18445|Torrens Formation|67354|5|Briefly described|p102 Fig.33.|Roadian|Roadian|||||Overlies Fossil Head Formation. Is overlain by Pearce Formation.||
18445|Torrens Formation|67370|6|Mentioned|p314 Fig.3, p316 Fig.5. |Permian|Permian|||Unit in Hyland Bay Subgroup.||Overlies Fossil Head Formation. Is overlain by Pearce Formation.||
18445|Torrens Formation|69452|5|Briefly described|p36:15, 20|Permian|Permian|Gorter (1998); given Formation status in Gorter et al. (2009) [?]. Bonaparte Basin. Very little information available. 22m thick in drillhole Torrens-1 and has limited areal distribution. Not included in the original Hyland Bay Formation (Mory, 1988).||||||12-JUL-16
18445|Torrens Formation|69454|5|Briefly described|p38:4|Wordian|Roadian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
18445|Torrens Formation|69653|6|Mentioned|p10|Guadalupian|Guadalupian|Petrel Sub-basin.||Hyland Bay Sub-group.||Overlies Fossil Head Formation. Is overlain by Pearce Formation.||
18445|Torrens Formation|69673|6|Mentioned|p153 fig 125, p173|||||Hyland Bay Subgroup||Overlain by Pearce Formation, overlies Fossil Head Formation||
18445|Torrens Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3, p2|Wordian|Wordian|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 Fossil Head Formation. Is overlain by Pearce Formation.||12-JUL-16
18445|Torrens Formation|72505|5|Briefly described|p890|Wordian|Roadian|Southern Bonaparte Basin. Correlated to the Dulhuntyispora granulata to didecitreletes ericanus zone.||||Overlies the Fossil Head Formation. Overlain by the Pearce Limestone.||
18515|Townsend Quartzite|22496|6|Mentioned|p10||Neoproterozoic|In the Officer Basin.||||||12-DEC-06
18515|Townsend Quartzite|22716|6|Mentioned|table4, p238|Cryogenian|Cryogenian|Age: 830 Ma. Part of sequence 1 of Centralian Superbasin.||||||
18515|Townsend Quartzite|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
18515|Townsend Quartzite|23282|6|Mentioned|p50|||May be a synonym of Pindyin Sandstone.||||||
18515|Townsend Quartzite|23288|5|Briefly described|p137|||||||||
18515|Townsend Quartzite|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|23571|4|Described|p7|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Unconformably underlain by Musgrave Complex. Disconformably overlain by Lefroy Formation and Browne Formation.||||||12-DEC-06
18515|Townsend Quartzite|23621|5|Briefly described|p33|||Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24067|5|Briefly described|p251|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24161|4|Described|p6, p27|Neoproterozoic|Neoproterozoic|Unconformably overlies the Mission Group. Overlain by the Lefroy Formation. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|24173|5|Briefly described|p24|Neoproterozoic|Neoproterozoic|Part of extensive sand blanket which includes Mount Kinahan Sandstone, Vaughan Springs Quartzite, Heavitree Quartzite and Lewis Range Sandstone (Redcliff Pound Group).  Geological Province: Officer Basin.||||||12-DEC-06
18515|Townsend Quartzite|24244|6|Mentioned|p3|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
18515|Townsend Quartzite|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Age: ~ 800 Ma.||||||
18515|Townsend Quartzite|30218|6|Mentioned|p404|||||||||
18515|Townsend Quartzite|30385|6|Mentioned|p8|||Also Table 1||||||
18515|Townsend Quartzite|30386|4|Described|p7|||Table 1 p7. Proterozoic age.||||||12-DEC-06
18515|Townsend Quartzite|30388|6|Mentioned|p9|||Middle Proterozoic age||||||
18515|Townsend Quartzite|30390|4|Described|p81|||See also p82-84.||||||12-DEC-06
18515|Townsend Quartzite|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup||||||
18515|Townsend Quartzite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18515|Townsend Quartzite|31457|4|Described|Table 2|||Mention p6.||||||12-DEC-06
18515|Townsend Quartzite|31460|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18515|Townsend Quartzite|31632|4|Described|Table 2|||See also p10.||||||12-DEC-06
18515|Townsend Quartzite|31635|6|Mentioned|Table 2|||||||||
18515|Townsend Quartzite|31636|6|Mentioned|Table 2|||||||||
18515|Townsend Quartzite|31914|1|Redefined|p95|Neoproterozoic|Mesoproterozoic|Middle to Upper ProterozoicM - U.||||||24-SEP-08
18515|Townsend Quartzite|31967|6|Mentioned|p.4|||||||||
18515|Townsend Quartzite|31973|6|Mentioned|p3|||Refers Lowry et al. (1971)||||||
18515|Townsend Quartzite|32727|5|Briefly described|p10|||Strat. and dates.||||||12-DEC-06
18515|Townsend Quartzite|33468|6|Mentioned|p212|||See also p214.||||||12-DEC-06
18515|Townsend Quartzite|33478|6|Mentioned|p454|||||||||
18515|Townsend Quartzite|34917|6|Mentioned|p12|||||||||
18515|Townsend Quartzite|35308|6|Mentioned|p454|||||||||
18515|Townsend Quartzite|36096|6|Mentioned|Fig.3|||||||||
18515|Townsend Quartzite|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18515|Townsend Quartzite|36886|4|Described|p197|||||||||
18515|Townsend Quartzite|36888|4|Described|p216|||||||||
18515|Townsend Quartzite|37299|6|Mentioned|Fig.1|||||||||
18515|Townsend Quartzite|37460|4|Described|p176|||||||||
18515|Townsend Quartzite|37707|6|Mentioned|p24|||||||||
18515|Townsend Quartzite|38157|6|Mentioned|Table VIII|||||||||
18515|Townsend Quartzite|38898|6|Mentioned|p83|||||||||
18515|Townsend Quartzite|39120|6|Mentioned|p146|||||||||
18515|Townsend Quartzite|39565|6|Mentioned|p31|||||||||
18515|Townsend Quartzite|40309|6|Mentioned|p91|||||||||
18515|Townsend Quartzite|41405|5|Briefly described|p205|||||||||
18515|Townsend Quartzite|43442|6|Mentioned|p17,19||Neoproterozoic|Age: c.820 Ma (Korsch & Kennard,1991).||||||12-DEC-06
18515|Townsend Quartzite|43692|6|Mentioned|p144|||||||||
18515|Townsend Quartzite|43697|6|Mentioned|p28|||||||||
18515|Townsend Quartzite|43732|6|Mentioned|p3|||||||||
18515|Townsend Quartzite|43756|6|Mentioned|p541|||||||||
18515|Townsend Quartzite|44109|5|Briefly described|p81, p164|||Of the Bentley Supergroup. Overlies the Tollu Group. Unconformably overlies the Musgrave Block units.  Possibly equivalent to Heavitree Quartzite.||||||
18515|Townsend Quartzite|44111|6|Mentioned|p.58|||in Officer Basin. Is lithologically similar to Coondra Formation (Savory Basin) and Googhenama Formation (Paterson Orogen).||||||
18515|Townsend Quartzite|44139|5|Briefly described|p286, 284, 285 Fig.3-69|||Overlies Musgrave-Mann Complex and Mission Group, Bentley Supergroup and also Scamp, Palgrave and Skirmish Hill (acid volcanic and granite) Cauldrons. Thick to thin-bedded flaggy sandstone overlain by coarse-grained, thick to very thick-bedded sandstone with large-scale cross-bedding.|| ||||06-MAR-18
18515|Townsend Quartzite|45149|2|Defined|p21|Proterozoic|Proterozoic|See also p3 and Table 1.||||||12-DEC-06
18515|Townsend Quartzite|45155|6|Mentioned|p18|||||||||
18515|Townsend Quartzite|46975|6|Mentioned|p83|||||||||
18515|Townsend Quartzite|49792|5|Briefly described|Fig.5|||||||||12-DEC-06
18515|Townsend Quartzite|49833|6|Mentioned|p8|||||||||
18515|Townsend Quartzite|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~800Ma.  Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|50204|6|Mentioned|p51|Neoproterozoic|Neoproterozoic|Of the Officer Basin.||||||
18515|Townsend Quartzite|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin.||Unit in Buldya Group.||Is overlain by Lefroy Formation conformably and locally unconformably.|Sandstone.|02-MAR-15
18515|Townsend Quartzite|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Age: ~800Ma. Geological Province: Officer Basin.||||||11-APR-08
18515|Townsend Quartzite|61272|5|Briefly described|p120, p123 Fig.4|||Unconformably overlies the Musgrave Complex and unconformably overlain by the Lefroy Group.||||||
18515|Townsend Quartzite|61560|5|Briefly described|p496|Neoproterozoic|Neoproterozoic|Contains the Skirmish impact structure.  Age is Early Neoproterozoic. On COOPER 1:250 000 sheet.||||||
18515|Townsend Quartzite|61732|5|Briefly described|p4 Fig. 3|Willouran|Willouran|Geological Province: central Officer Basin.||||||07-FEB-11
18515|Townsend Quartzite|62453|3|Fully described|p5 Fig. 3, 14|Cryogenian|Tonian|Of Buldya Gp. Geol. Prov: Officer Basin. Overlies: Bently Supergroup. Previous usage is Townsend Range Series, Townsend Fm, Townsend quartzite. Synonym with Pidyin Sandstone. Overlain by Lefroy Fm, Browne Fm. Sandstone. Uncon. overlies: Musgrave Cplx.||||||
18515|Townsend Quartzite|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
18515|Townsend Quartzite|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
18515|Townsend Quartzite|64325|5|Briefly described|p82 Fig. 2|Neoproterozoic|Neoproterozoic|Basal unit of Supersequence 1. Conformably overlain by Lefroy Formation. Geological Province: western Officer Basin. Sandstone unit. Contains fluvial to nearshore marine sandstones.||||||11-JUL-13
18515|Townsend Quartzite|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.||||||09-DEC-08
18515|Townsend Quartzite|64625|6|Mentioned|p246|||Basal clastic sediments of the Centralian Superbasin.|>c.830 Ma.|||||
18515|Townsend Quartzite|64793|6|Mentioned|p283-285 figs 2,3,4; p291 fig 8|Cryogenian|Cryogenian|Of central Officer Basin. Age inferred from Fig.3.|c.840 -c.838 Ma.|||Is overlain unconformably by Browne Formation.||
18515|Townsend Quartzite|64796|6|Mentioned|p183 fig 2|Neoproterozoic|Neoproterozoic|Of Officer Basin||||||
18515|Townsend Quartzite|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
18515|Townsend Quartzite|64970|4|Described|p718, p719 Fig. 2, p721 Fig. 6|Neoproterozoic|Neoproterozoic|Is overlain by Lefroy, Browne, Hussar, Kanpa and Steptoe Formations in places. Massive, pink to white, very hard, quartz sandstone. Geological Province: Officer Basin.||||||
18515|Townsend Quartzite|65102|4|Described|p363,364, 365, 366, 367,372, Figs.4-43|Neoproterozoic|Neoproterozoic|Paterson Orogen (SE) and Officer Basin. 100-370m. Quartz to feldspathic arenite, shale beds; minor conglomerate; marine, mainly littoral-sublittoral with possible deltaic influence; unconformable over granitic basement; type section 38km E of Ainslie Gorge; date on underlying Tollu Volcanics: 1060+/-140 Ma.||||||
18515|Townsend Quartzite|65338|6|Mentioned|p59.|||Officer Basin. Correlated with Vaughan Springs Quartzite.||||||
18515|Townsend Quartzite|65363|6|Mentioned|p5 Fig.4, p11.|Neoproterozoic|Neoproterozoic|North-central Officer Basin.||Unit in Buldya Group.||||
18515|Townsend Quartzite|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group. Central Officer Basin.||||||19-MAR-12
18515|Townsend Quartzite|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group, central Officer Basin||||||
18515|Townsend Quartzite|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin. May be equivalent to Heavitree Quartzite in the Amadeus Basin. Part of Supersequence 1.||||||
18515|Townsend Quartzite|65416|5|Briefly described|p137, p138 Fig.3, p140, p145.|Late Proterozoic|Late Proterozoic|Crops out along the southwest margin of the Musgrave Complex. Officer Basin. Lateral equivalent of Heavitree Quartzite (Amadeus Basin). Part of Sequence LP1A of Supersequence PL1. Transgressive: fluvial to shallow marine. Correlated with Glass Spring Formation in the Savory Sub-basin.||||Unconformably overlies Musgrave Complex. Is overlain by Browne Formation unconformably and conformably/gradationally by Lefroy Formation.|Orthoquartzite.|
18515|Townsend Quartzite|66281|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.|||||Laminated to very thickly-bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
18515|Townsend Quartzite|66282|6|Mentioned|Map legend.|||Officer Basin. No outcrop on map; interpreted bedrock geology only.||||||
18515|Townsend Quartzite|67128|5|Briefly described|p33|||Represents the base of the Officer Basin at the SW edge of the Musgrave Province. Has distinctly different provenance from MacDougall Formation.|c.1134 Ma (maximum depositional age).|||||
18515|Townsend Quartzite|67195|5|Briefly described|p9 fig 5, p10, p19 tbl 1, p20, 40, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 4.45 W/mK. Basal unit of one well in this study. See also App 1.||||Overlain by Lefroy Formation, unconformably overlain by Browne Formation|Quartzite.|04-JAN-23
18515|Townsend Quartzite|67244|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin. Described together with Lefroy Formation.||Unit in Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|21-NOV-13
18515|Townsend Quartzite|67375|6|Mentioned|p38 Table 1. |||||||Conformably overlies Mission Group.||
18515|Townsend Quartzite|67553|6|Mentioned|p40|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin.||||Underlain by Milesia Formation/Mission Group.||
18515|Townsend Quartzite|68270|5|Briefly described|p678|||Western Officer Basin.||||Overlain disconformably by Lupton Formation.||
18515|Townsend Quartzite|68733|6|Mentioned|p190|||Northern and western Officer Basin.||||||06-DEC-17
18515|Townsend Quartzite|68995|6|Mentioned|p19, p20|||Officer Basin.||||Overlies the Milesia Formation.||
18515|Townsend Quartzite|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
18515|Townsend Quartzite|69029|6|Mentioned|p329|Neoproterozoic|Neoproterozoic|Of Officer Basin.||||Overlain by Lefroy Formation.||
18515|Townsend Quartzite|69091|4|Described|p34-35, p43, p44, see comments|Neoproterozoic|Neoproterozoic|Basal unit of western Officer Basin, cropping out at northeastern edge of basin. It has limited distribution (not found in drillholes further southwest). Brought to present-day surface by reactivated Winduldarra Fault. See also p106 Fig.5.7a, p107 Fig.5.8a, p109 Fig.5.10, p182, p184.||Buldya Group||Overlies Bentley Supergroup; overlies Mission Group.||
18515|Townsend Quartzite|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Cryogenian|Neoproterozoic|Officer Basin, Centralian Superbasin. Lithology description shared with Lefroy Formation. Sample description includes: sandstone, pebbly sandstone and conglomerate.||Buldya Group|||Quartz arenite and feldspathic arenite; minor conglomerate and shale beds|
18515|Townsend Quartzite|70018|6|Mentioned|p240|||Officer Basin.||||||
18515|Townsend Quartzite|70134|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and  shale beds; medium- to large-scale cross-bedding; commonly intensely silicified.|
18515|Townsend Quartzite|70137|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin. The two facies are mapped separately.||Buldya Group.||Overlies Milesia Formation.|Laminated to very thickly bedded, well sorted, medium- to coarse-grained quartz arenite and feldspathic arenite, minor conglomerate and shale beds, commonly intensely silicified; poorly exposed cobble and boulder conglomerate, lesser sandstone.|
18515|Townsend Quartzite|70634|4|Described|100k_geologyp_lut.csv|Cryogenian|Cryogenian|Says age Cryogenian, 850-635 Ma inferred or biostratigraphic.|||||Laminated to very thickly bedded, well sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|30-AUG-18
18515|Townsend Quartzite|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_interpgeop_lut.csv.|1000-800 Ma (inferred)|Unit of Buldya Group.|||Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; vobble and boulder conglomerate, and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|
18515|Townsend Quartzite|71211|6|Mentioned|p235|||||||Conformably or unconformably overlies the Mission Group.||
18515|Townsend Quartzite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Buldya Group.|||Laminated to very thick bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; minor conglomerate and shale beds; medium- to large-scale cross-bedding.|
18515|Townsend Quartzite|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). Deposited in braided fluvial to nearshore marine environments. Sample GSWA 189557 (quartz sandstone) yielded a weighted mean 207Pb/206Pb age of 1134+\-19 Ma, interpreted to be maximum depositional age of the sandstone. Sample GSWA 195237 (lithic sandstone) yielded a concordia age of 1134+\5 Ma, interpreted as maximum depositional age of the sedimentary protolith.See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1000-800 Ma (inferred0|Unit of Buldya Group.||Lowermost unit of Buldya Group. Overalin by Lefroy Formation or Browne Formation. Underlain by Bentley Supergroup.|Laminated to very thickly bedded, well-sorted, medium- to coarse-grained quartz arenite and feldspathic arenite; cobble and boulder conglomerate and shale beds; medium- to large-scale cross-bedding; commonly intensely silicified|
18515|Townsend Quartzite|72094|4|Described|p4, p5|Neoproterozoic|Neoproterozoic|Officer Basin. Outcrops of NW-trending ridges in the Officer Basin. Misspelt(?) as Townshend Qtz on  p5||Unit of Buldya Group||Underlain by Mission Group apparently concordantly in Warburton area.|Laminated to very thick-bedded, well-sorted, medium to coarse-grained quartz arenite and feldspathic arenite.|
18531|Traine Formation|30525|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18531|Traine Formation|30533|4|Described|Table 5|||||||||
18531|Traine Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18531|Traine Formation|30896|4|Described|p19|||||||||
18531|Traine Formation|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18531|Traine Formation|32660|5|Briefly described|Table 6|||||||||
18531|Traine Formation|32728|6|Mentioned|Table 7|||||||||
18531|Traine Formation|34462|4|Described|Table 1|||Adelaidean. See P10||||||
18531|Traine Formation|34463|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18531|Traine Formation|36551|6|Mentioned|Table 10|||||||||
18531|Traine Formation|36898|6|Mentioned|p191|||||||||
18531|Traine Formation|37927|5|Briefly described|p508|||||||||
18531|Traine Formation|38157|6|Mentioned|Table X|||||||||
18531|Traine Formation|39210|5|Briefly described|Fig.18|||||||||
18531|Traine Formation|41429|6|Mentioned|p247|||||||||
18531|Traine Formation|42149|6|Mentioned|Table 1 P709|||||||||
18531|Traine Formation|42710|5|Briefly described|map legend|Proterozoic||||||||
18531|Traine Formation|42811|4|Described|p31|||of Mount House Group||||||
18531|Traine Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount House area. 10-60 m thick.||Mount House Group||Overlies Walsh Tillite conformably. Is conformably overlain by Throssell Shale.|Ferruginous and dolomitic sandstone.|
18531|Traine Formation|44366|14|Not recorded|p.17, Table 3||Adelaidean|Part of Mount House Group. Definition on Tech.File E/52-5.||||||
18531|Traine Formation|44367|14|Not recorded|map legend||Adelaidean|(Reprinted 1971).||||||
18531|Traine Formation|48931|4|Described|p61|||||||||
18531|Traine Formation|63458|6|Mentioned|p873 Fig.2, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Mount House Group.||||
18531|Traine Formation|67563|6|Mentioned|p120 Fig.1|||||||||
18531|Traine Formation|68244|4|Described|p660-662|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. No evidence of glaciogenic influence.||Unit of Mount House Group.||Overlain by Throssell Shale. Underlain by Walsh Formation.|Massive, medium- to coarse-grained lithic sandstone; dolomitic.|
18531|Traine Formation|68473|6|Mentioned|p531|||||Mount House Group||||
18531|Traine Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Mount House Sub-basin, Louisa Basin.||Mount House Group|||Green to brown, coarse-grained, lithic sandstone with minor sandy dolomite and dolomitic sandstone; scattered glacial erratics up to 2.5 m diameter.|04-AUG-15
18531|Traine Formation|69634|4|Described|GEOL_LUT_CSV files|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 Mount House Group.|||Green to brown, coarse-grained, lithic sandstone with minor sandy dolomite and dolomitic sandstone; scattered glacial erratics up to 2.5 m diameter|
18531|Traine Formation|69660|5|Briefly described|Map legend|Ediacaran|Ediacaran|Louisa Basin, North Australian Craton.||Unit in Mount House Group.|||Green to brown, coarse-grained lithic sandstone with minor sandy dolomite and dolomitic sandstone; scattered glacial erratics up to 2.5 m diameter.|
18531|Traine Formation|70154|4|Described|250k_geologyp_lut.csv|Ediacaran|Ediacaran|See also 250k_interpgeop_lut.csv.|541-635 Ma|Mount House Group|||Green to brown, coarse-grained, lithic sandstone with minor sandy dolomite and dolomitic sandstone; scattered glacial erratics up to 2.5 m diameter|
18531|Traine Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|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 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|635-541 Ma (inferred)|Unit of Mount House Group.|||Green to brown coarse lithic sandstone with minor sandy dolomite and dolomitic sandstone, and scattered glacial erratics|
18531|Traine Formation|71811|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Louisa Basin.||Mount House Group.|||Green to brown, coarse-grained, lithic sandstone with minor sandy dolomite and dolomitic sandstone; scattered glacial erratics up to 2.5m diameter.|
18532|Trainor Hill Sandstone|22746|5|Briefly described|Fig.3 p515|Middle Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|22922|5|Briefly described|34|||||||||
18532|Trainor Hill Sandstone|23282|1|Redefined|p79||Middle Cambrian|of Krieg (1973) and defined by Benbow (1982). May be equiv to part of 'Wirrildar beds' and Moodlatana Formation. Age: Middle Cambrian 516-510Ma. of Marla Group, Officer Basin.||||||
18532|Trainor Hill Sandstone|23288|6|Mentioned|Fig.5|Late Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|23524|5|Briefly described|p221 Fig. 3|Middle Cambrian|Middle Cambrian|||||||
18532|Trainor Hill Sandstone|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
18532|Trainor Hill Sandstone|24112|5|Briefly described|p254 Fig.2|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin||||||
18532|Trainor Hill Sandstone|30544|6|Mentioned|p49|||||||||
18532|Trainor Hill Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
18532|Trainor Hill Sandstone|31455|6|Mentioned|p12|||||||||
18532|Trainor Hill Sandstone|31698|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|?Middle to Upper CambrianM? - U||||||
18532|Trainor Hill Sandstone|35628|4|Described|Table 3|||See also P14.||||||
18532|Trainor Hill Sandstone|36096|6|Mentioned|Fig.3|||||||||
18532|Trainor Hill Sandstone|36109|6|Mentioned|Fig.2|||||||||
18532|Trainor Hill Sandstone|36491|6|Mentioned|Fig.2|||||||||
18532|Trainor Hill Sandstone|36920|6|Mentioned|Table 1|||||||||
18532|Trainor Hill Sandstone|38022|6|Mentioned|Fig.4|||||||||
18532|Trainor Hill Sandstone|38329|1|Redefined|p205|Cambrian|Cambrian|||||||
18532|Trainor Hill Sandstone|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
18532|Trainor Hill Sandstone|40945|6|Mentioned|Fig.3|||||||||
18532|Trainor Hill Sandstone|41276|6|Mentioned|Fig.1|||||||||
18532|Trainor Hill Sandstone|43052|5|Briefly described|Fig.2.10|||||||||
18532|Trainor Hill Sandstone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Marla Group. Deltaic sandstone, siltstone and shale.||||||25-MAY-05
18532|Trainor Hill Sandstone|43258|5|Briefly described|Map Legend||Cambrian|||||||
18532|Trainor Hill Sandstone|43298|5|Briefly described|Map Legend||Cambrian|||||||
18532|Trainor Hill Sandstone|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
18532|Trainor Hill Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
18532|Trainor Hill Sandstone|43732|6|Mentioned|Fig.4,p5||Middle Cambrian|||||||
18532|Trainor Hill Sandstone|43743|6|Mentioned|Fig.2,p33||Middle Cambrian|||||||
18532|Trainor Hill Sandstone|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Geological Province: central Officer Basin.||||||
18532|Trainor Hill Sandstone|44133|4|Described|p39, 42, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the Marla Group. Overlies: Apamurra Formation. Contact with Mount Johns Conglomerate. Underlies: Byilkaoora Formation.||||||07-NOV-08
18532|Trainor Hill Sandstone|45149|6|Mentioned|Table 1|||Page 15.||||||
18532|Trainor Hill Sandstone|49792|5|Briefly described|Fig.5|||||||||
18532|Trainor Hill Sandstone|60565|5|Briefly described|p20 Fig.3b|||Overlies the Apamurra Formation.||||||
18532|Trainor Hill Sandstone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Deltaic sandstone, siltstone and shale; fan-delta conglomerate and sandstone.||||||
18532|Trainor Hill Sandstone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Deltaic sandstone, siltstone and shale; fan-delta conglomerate and sandstone.||||||
18532|Trainor Hill Sandstone|61732|6|Mentioned|p79, p82 Fig. 33|Cambrian|Cambrian|Geological Province: Birksgate Sub-basin.||||||07-FEB-11
18532|Trainor Hill Sandstone|62570|5|Briefly described|p580 Figs. 2 and 3|Middle Cambrian|Middle Cambrian|Of the Marla Group. Geological Province: Officer Basin. Feldspathic sandstone.||||||13-SEP-18
18532|Trainor Hill Sandstone|65313|5|Briefly described|p577, p578 Fig 6, p 573 Fig. 2|Late Cambrian|Middle Cambrian|Previously dated ca 500 Ma, now confirmed as 'no younger than mid-Late Cambrian', paleosols identified in section in Byilkaoora 2 borehole - Officer Basin.||Of Marla Group.||Overlies Apamurra Formation.||26-MAR-12
18532|Trainor Hill Sandstone|67120|5|Briefly described|Map legend|Cambrian|Cambrian|||Marla Group|||Sandstone, red-brown, fine-grained, cross-bedded; siltstone to claystone, red, micaceous; basal very fine-grained sandstone.|
18532|Trainor Hill Sandstone|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em5.|||||Mostly non-marine sandstone, siltstone, claystone and minor dolomite, limestone, chert and conglomerate.|
18532|Trainor Hill Sandstone|67921|5|Briefly described|Map legend|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone; cross-bedded; soft sediment disruption including roll slumps; thin mudstone interbeds and locally some clay intraclasts.|
18532|Trainor Hill Sandstone|69445|5|Briefly described|p30:5, 17|||Officer Basin.||||Is overlain by Kulyong Formation (now Table Hill Volcanics).||12-JUL-16
18532|Trainor Hill Sandstone|70336|5|Briefly described|Map legend|Cambrian|Cambrian|||Of Marla Group.|||Red-brown, fine-grained, cross-bedded sandstone; red, micaceous siltstone to claystone; basal very fine-grained sandstone.|12-JAN-16
18532|Trainor Hill Sandstone|70839|5|Briefly described|p342-343,345|Early Cambrian|Early Cambrian|Of East Officer Basin. Late early Cambrian age based on stratigraphic position within biostratigraphically dated succession and revised radiometric age of overlying Table Hill Volcanics (Morton and Drexel, 1997; Jourdan et al., 2014).||||Overlain by Table Hill Volcanics.||
18532|Trainor Hill Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
18532|Trainor Hill Sandstone|71618|6|Mentioned|p130|||Of Officer Basin.||||||
18532|Trainor Hill Sandstone|72478|6|Mentioned|p8, p11|Middle Cambrian|Early Cambrian|Officer Basin. See also p51, 69, Fig.7 p70 [of the document].|c. 516 Ma-510 Ma|Marla Group||||29-MAR-21
18532|Trainor Hill Sandstone|73090|5|Briefly described|p12 Fig.7|Cambrian|Cambrian|||Marla Group.|||Sandstone, red-brown, fine-grained, cross-bedded; siltstone to claystone, red, micaceous; basal very fine-grained sandstone.|
18532|Trainor Hill Sandstone|73099|5|Briefly described|Map legend.|Middle Cambrian|Early Cambrian|Officer Basin.||Marla Group.||Overlies Apamurra Formation. Is overlain by Mount Chandler Sandstone (Munda Group).|Pale grey, white and yellow-brown, fine- to coarse-grained, micaceous, feldspathic quartz sandstone with numerous interbeds of green-grey and red-brown micaceous siltstone and claystone.|
18532|Trainor Hill Sandstone|73100|5|Briefly described|Map legend|Cambrian|Cambrian||||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone; trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds, clay intraclasts locally.|
18532|Trainor Hill Sandstone|73109|5|Briefly described|Map legend.|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone, locally with red mottling or diffuse pale colourations; trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds; clay intraclasts locally.|
18532|Trainor Hill Sandstone|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Subcrop and minor outcrop.|||||Fine- to medium-grained, kaolinitic, micaceous and lithic white quartz sandstone, local red mottling or diffuse pale colourations; low angle trough or angular cross-bedding; soft sediment disruption; thin mudstone interbeds; local clay intraclasts.|
18563|Trealla Limestone|12471|6|Mentioned|p475 Fig.2.|Neogene|Neogene|Middle Miocene. There is a time-break at the base of this unit, related to tectonism due to the collision of Australia with Asia.||||Overlies Cardabia Calcarenite. ?||24-OCT-14
18563|Trealla Limestone|12729|6|Mentioned|p9 Fig.6, p17.|Miocene|Miocene|Eolian (Hocking et al., 1987).||||Adjacent to the Pindilya Formation.|Limestone.|
18563|Trealla Limestone|13615|3|Fully described|p4-p5, p20, p33, p36|Late Miocene|Middle Miocene|Peedamullah Shelf. 20-30m thick. Spores/Pollen Zone and Dinoflagellate zones provided. Deposited in a shallow marine environment in a middle to inner shelf setting. Intersected in numerous drillholes. Type section occurs at Mount Lefroy; 23deg13'00"s 114deg00'20"E. Age derived from fossil assemblage. See also p38, p40, p42, p56, p62, p65, p101.||Cape Range Group||Unconformably overlies the Cardabia Group.|Commonly pure calcirudite, calcarenite and calcisiltite.|11-FEB-19
18563|Trealla Limestone|14228|5|Briefly described|p5 Fig.2, p9, p16|Miocene|Miocene|Gascoyne Platform.||Cape Range Group|||Flat-lying shallow-marine carbonate strata.|
18563|Trealla Limestone|23311|5|Briefly described|map legend|Miocene|Miocene|||||||
18563|Trealla Limestone|23312|5|Briefly described|map legend|Miocene|Miocene|||||||
18563|Trealla Limestone|23403|4|Described|p9|Miocene|Miocene|||||||24-NOV-09
18563|Trealla Limestone|23520|5|Briefly described|p12. p30|Cenozoic|Cenozoic|Geological Province:  Abrolhos Sub-basin.||||||19-NOV-08
18563|Trealla Limestone|23572|5|Briefly described|p8 Fig. 6|Miocene|Miocene|Geological Province: Carnarvon Basin.||||||
18563|Trealla Limestone|23620|5|Briefly described|p4 Fig. 4|Neogene|Neogene|Marine limestone and minor marine and continental sandstone.||||||01-SEP-08
18563|Trealla Limestone|23726|5|Briefly described|p88|Middle Miocene|Oligocene|Overlying unit Peron Sandstone. Underlying unit Tulki Limestone. Geological Province: Carnarvon Basin.||||||
18563|Trealla Limestone|23815|4|Described|p303|Miocene|Miocene|Age: Middle Miocene. Geological Province: Carnarvon Basin. Overlying unit: Exmouth Sandstone. Underlying units: Tulki Limestone, Mandu Calcarenite and Giralia Calcarenite (disconformable). Max. thickness: 55 m. Fossiliferous.||||||27-APR-05
18563|Trealla Limestone|23816|6|Mentioned|p254|Early Miocene|Early Miocene|Geological Province: Carnarvon Basin.||||||
18563|Trealla Limestone|23935|5|Briefly described|p11 Fig.7|Miocene|Miocene|Geological Province: Southern Carnarvon Basin.||||||
18563|Trealla Limestone|23976|5|Briefly described|Map Legend|Neogene|Neogene|||||||
18563|Trealla Limestone|23977|5|Briefly described|Map Legend|Neogene|Neogene|||||||
18563|Trealla Limestone|23978|5|Briefly described|Map Legend|Neogene|Neogene|||||||
18563|Trealla Limestone|24059|5|Briefly described|p132|Tertiary|Tertiary|Geological Province: Barrow Sub-basin.||||||
18563|Trealla Limestone|24084|5|Briefly described|p146 Fig.2|Miocene|Miocene|Geological Province: North Carnarvon Basin.||||||16-MAR-05
18563|Trealla Limestone|24351|5|Briefly described|Plate 4 (in pocket)|Middle Miocene|Middle Miocene|Geological Province: Exmouth Sub-basin and Gascoyne Platform/Sub-basin.||||||13-DEC-07
18563|Trealla Limestone|24541|4|Described|p61|Middle Miocene|Middle Miocene|Of the Cape Range Group. Geological Province: Northern Carnarvon Basin.||||||
18563|Trealla Limestone|24543|5|Briefly described|Map legend|Miocene|Miocene|Of the Cape Range Group.  Calcirudite, calcarenite and calcisiltite.||||||
18563|Trealla Limestone|30110|6|Mentioned|p81|||Lower Miocene age.||||||
18563|Trealla Limestone|30122|4|Described|p49|||See also P50.||||||
18563|Trealla Limestone|30304|6|Mentioned|p47|||Miocene, part of Cape Range Group. See also Fig3||||||24-OCT-14
18563|Trealla Limestone|30504|6|Mentioned|p34|||||||||
18563|Trealla Limestone|30821|5|Briefly described|p59|||Stratigraphic sequence on table.||||||
18563|Trealla Limestone|31561|6|Mentioned|p6|||Early Miocene||||||
18563|Trealla Limestone|32166|6|Mentioned|p159|||||||||
18563|Trealla Limestone|32648|6|Mentioned|p32|||in Cape Range Gp.||||||
18563|Trealla Limestone|32750|6|Mentioned|p309|||Tertiary section||||||
18563|Trealla Limestone|33386|6|Mentioned|Fig.7|||||||||
18563|Trealla Limestone|33450|6|Mentioned|Fig.5|||See P11.||||||
18563|Trealla Limestone|33453|6|Mentioned|p72|||Strat.||||||
18563|Trealla Limestone|34363|6|Mentioned|p56|||See also P57. Lower Miocene.||||||
18563|Trealla Limestone|35105|6|Mentioned|Fig.5|||||||||
18563|Trealla Limestone|35144|6|Mentioned|p5|||||||||
18563|Trealla Limestone|35282|6|Mentioned|Fig.2|||||||||
18563|Trealla Limestone|36257|6|Mentioned|Table 2.1|||||||||
18563|Trealla Limestone|36890|3|Fully described|p303|||See also p254.||||||08-APR-16
18563|Trealla Limestone|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
18563|Trealla Limestone|39427|4|Described|Table 1|||||||||
18563|Trealla Limestone|40343|5|Briefly described|p12|||||||||
18563|Trealla Limestone|40366|6|Mentioned|p91|||||||||
18563|Trealla Limestone|40617|6|Mentioned|p16|||Mention P18||||||
18563|Trealla Limestone|40800|6|Mentioned|p26|||||||||
18563|Trealla Limestone|41271|3|Fully described|p181|||||||||
18563|Trealla Limestone|41437|6|Mentioned|p76|||||||||
18563|Trealla Limestone|41439|6|Mentioned|p124|||||||||
18563|Trealla Limestone|41712|6|Mentioned|Fig.8|||||||||
18563|Trealla Limestone|41729|6|Mentioned|Fig.2|||||||||
18563|Trealla Limestone|41732|6|Mentioned|Fig.3|||||||||
18563|Trealla Limestone|42075|5|Briefly described|Fig.4 P245|||||||||
18563|Trealla Limestone|42116|6|Mentioned|p69|||||||||
18563|Trealla Limestone|42395|6|Mentioned|Fig.22 P85|||||||||
18563|Trealla Limestone|42615|5|Briefly described|p8|||Middle Miocene||||||
18563|Trealla Limestone|43724|6|Mentioned|Fig.15,p65||Miocene|||||||
18563|Trealla Limestone|44491|14|Not recorded|map legend||Early Miocene|Lower Miocene.||||||
18563|Trealla Limestone|44492|14|Not recorded|p.9,opp.p.4, map||Early Miocene|(F50-1,2). L.Miocene. Fauna "indicative of marine shallow-meritic to littoral facies" (p.9).||||||
18563|Trealla Limestone|44532|4|Described|p.9,10, map|||(G50-5).||||||
18563|Trealla Limestone|44533|5|Briefly described|map legend||Miocene|Miocene.||||||
18563|Trealla Limestone|44537|14|Not recorded|map legend||Miocene|||||||
18563|Trealla Limestone|44657|14|Not recorded|p.5,6,13,14,15|||||||||
18563|Trealla Limestone|44959|3|Fully described|p.25|||||||||
18563|Trealla Limestone|45015|5|Briefly described|map legend||Tertiary|Of the Cape Range Group. Age is Late Tertiary.||||||01-JUN-06
18563|Trealla Limestone|45142|6|Mentioned|p25|||See also Fig.4.||||||
18563|Trealla Limestone|46805|6|Mentioned|p171|||||||||
18563|Trealla Limestone|46950|6|Mentioned|Fig.15|||||||||
18563|Trealla Limestone|46983|6|Mentioned|Fig.2|||||||||
18563|Trealla Limestone|48610|14|Not recorded|p14,Pl.1|||Salt Marsh area.||||||
18563|Trealla Limestone|48628|14|Not recorded|p23|||(F50-5/Onslow).||||||
18563|Trealla Limestone|48831|14|Not recorded|p.10,17,21||Early Miocene|Lower Miocene.||||||
18563|Trealla Limestone|49942|5|Briefly described|p4 Fig.3|Miocene|Miocene|Geological Province: Gascoyne Platform.||||||
18563|Trealla Limestone|60119|5|Briefly described|p25|Miocene|Miocene|||||||22-JUL-04
18563|Trealla Limestone|60384|6|Mentioned|p243, Fig 2a|Miocene|Miocene|Perth and Carnarvon Basins.||||||
18563|Trealla Limestone|60725|6|Mentioned|p36 Fig.6. |Miocene|Miocene|||||||
18563|Trealla Limestone|61155|5|Briefly described|p15|Middle Miocene|Middle Miocene|Of Cape Range Group. Overlies/interfingers with Pindilya Formation; also overlies Lamont Sandstone. Overlain by/interfingers with Pilgramunna Fm; and Bare Fm. Age: 17.5-10.5Ma. Max. thickness: 415m. Geological Province: Carnarvon Basin.||||||
18563|Trealla Limestone|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Of the Cape Range Group.||||||21-MAR-06
18563|Trealla Limestone|62734|5|Briefly described|p1362 Fig. 2|Miocene|Miocene|Geological Province: Barrow Sub-basin.||||||01-SEP-08
18563|Trealla Limestone|62837|5|Briefly described|Stratigraphic columns|Middle Miocene|Middle Miocene|Age: <15Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
18563|Trealla Limestone|63068|5|Briefly described|p44 Fig. 2|Miocene|Miocene|Geological Province: Carnarvon Basin.||||||
18563|Trealla Limestone|65194|5|Briefly described|p113|Middle Miocene|Middle Miocene|Up to 17 m of crystalline limestone with pale cream and yellow clay. Marine or lagoonal equivalent to Millstream Dolomite. Unconformably overlies Yarraloola Conglomerate.||||||
18563|Trealla Limestone|66125|6|Mentioned|p132, 138 Fig.10|Miocene|Oligocene|Onshore Carnarvon Basin. Tertiary.||||||
18563|Trealla Limestone|67200|5|Briefly described|p8 fig 6, p53|Miocene|Oligocene|Thermal conductivity of 1.68 W/mK||||Unconformably overlies Tulki Limestone, overlies Lamont Sandstone, overlain by Peron Sandstone, Pilgramunna Formation, Bare Formation|Crudely bedded limestone with invertebrate macrofossils.|
18563|Trealla Limestone|67368|6|Mentioned|p209 Fig.4.|Miocene|Miocene|||||Overlies Mandu Formation. Is overlain by Bare Formation.||
18563|Trealla Limestone|67970|5|Briefly described|p25 Fig.4.|Tortonian|Langhian|Exmouth Plateau.||Unit in Cape Range Group.||||
18563|Trealla Limestone|68811|6|Mentioned|p108 fig 62|Tertiary|Tertiary|See also informal references on p107, 191.||Of Cape Range Group.||||16-APR-20
18563|Trealla Limestone|69182|6|Mentioned|Ch3 p13, Ch3 p23-p26, Ch3 p71|||Carnarvon Basin.||Cape Range Group||Overlies the Mandu Calcarenite. Overlain by the Exmouth Sandstone.||
18563|Trealla Limestone|69297|5|Briefly described|p247, p249|Cenozoic|Cenozoic|Gascoyne Sub-basin of the Southern Carnarvon Basin.||||Unconformably overlies the Cardabia and Giralia Calcarenites.|Limestones.|
18563|Trealla Limestone|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Miocene|Miocene|See also. Northern Carnarvon Basin.||Cape Range Group.||Overlies Mandu Limestone. Is overlain by Delambre and Bare Formations .||
18563|Trealla Limestone|70906|5|Briefly described|p757|Miocene|Miocene|Gorgon Platform.||||Overlies Walcott Formation. Is overlain by Delambre Formation.||
18563|Trealla Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcilutite, calcirudite|
18566|Tredian Formation|30565|6|Mentioned|p120|||||||||
18603|Tripod Hill Member|23130|5|Briefly described|p348|||of Kambalda Komatiite. Overlies Silver Lake Member.||||||
18603|Tripod Hill Member|24325|5|Briefly described|p58|||Of the Kambalda Komatiite Formation (Kambalda Group). Geological Province: Kambalda Dome, Yilgarn Craton.||||||
18603|Tripod Hill Member|41662|6|Mentioned|p263|||||||||
18603|Tripod Hill Member|41670|5|Briefly described|p250|||||||||
18603|Tripod Hill Member|41890|5|Briefly described|Table 1|||Same as Tripod Hill Komatiite, Fig.3||||||
18603|Tripod Hill Member|43162|6|Mentioned|17|||||||||
18603|Tripod Hill Member|50548|5|Briefly described|p1174||Archean|Upper Member of Kambalda Komatiite Formation. Overlies Silver Lake Member.||||||07-FEB-11
18603|Tripod Hill Member|60514|5|Briefly described|p28|Archean|Archean|Of the Kambalada Komatiite. Overlain by Devon Consol Basalt, underlain by the Silver Lake Member. Maximum Thickness: 700m. Geological Province: Yilgarn Craton.||||||07-FEB-11
18603|Tripod Hill Member|60578|5|Briefly described|p5|Archean|Archean|Of Kambalda Komatiite. <10m thick spinifex textured flows.||||||13-JUN-17
18603|Tripod Hill Member|60623|4|Described|p28|Archean|Archean|Upper member of Kambalda Komatiite. Thin (0.5-10m) flows with total thickness of up to 700m. Conformably overlain by Devon Consols Basalt. Overlies Silver Lake Member.||||||07-NOV-08
18603|Tripod Hill Member|62110|5|Briefly described|p1442 Fig. 1|||Of the Kambalda Komatiite. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
18603|Tripod Hill Member|67198|4|Described|p81, p83, p85, p87|Neoarchean|Neoarchean|Thickness shown as 100-1000m and 50-500m. Thickest in the N and W flanks of the Kambalda Dome. Geochemistry described; shows LREE enrichment and lower MgO compared with Silver Lake Member.|2702 +/- 4 Ma|Kambalda Komatiite||Overlies Silver Lake Member. Is intruded by Kambalda Granodiorite|Characterised by thin (1-10m) well differentiated komatiite flow units. Flows exhibit well developed flow top breccia, spinifex texture zones and well developed B-zone cumulates. Only a few discontinuous sedimentary intervals.|11-SEP-17
18603|Tripod Hill Member|68289|5|Briefly described|p6-p7, p29-p31|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group.  50-500m thick. Referred to as the Tripod Hill Komatiite on p31 fig 22.||Kambalda Komatiite||Overlies the Silver Lake Member. Overlain by the Devon Consols Basalt. Intruded by the Kambalda Granodiorite.||
18603|Tripod Hill Member|69583|5|Briefly described|p37|||Southern Kalgoorlie Terrane. 50-500m thick.||Kambalda Komatiite.||||
18603|Tripod Hill Member|69631|5|Briefly described|p7, p25, p28|||Kambalda area, Kalgoorlie Terrane. 50-500m thick. Also appears as Tripod Hills Member on p25, and as Tripod Hill Komatiite on p28.||Kambalda Komatiite.||Overlies Silver Lake Member. Is overlain by Devon Consols Basalt.||
18603|Tripod Hill Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2709 - 2692 Ma (inferred).|Kambalda Komatiite|||Komatiite, upper unit; flows up to 20 m thick; peridotite to picrite; rare intersedimentary units; commonly serpentinized.|
18603|Tripod Hill 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).|2709-2692 Ma (inferred)|Unit of Kambalda Komatiite.|||Komatiite, upper unit; flows up to 20  m thick; peridotite to picrite; rare intersedimentary units; commonly serpentinized|
18604|Triumph Gabbro|41249|6|Mentioned|Fig.11|||||||||
18604|Triumph Gabbro|42221|6|Mentioned|Table 1 P6|||||||||
18604|Triumph Gabbro|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
18604|Triumph Gabbro|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
18604|Triumph Gabbro|43102|5|Briefly described|Fig.2|||||||||
18604|Triumph Gabbro|43162|6|Mentioned|5|||||||||
18604|Triumph Gabbro|43496|6|Mentioned|9|||Age: 2675+/-6Ma||||||
18604|Triumph Gabbro|60076|6|Mentioned|p13 Fig. 5|||||||||
18604|Triumph Gabbro|60514|6|Mentioned|p65 Table 1|Archean|Archean|Of the Black Flag Group. Geological Province: Kambalda Domain, Yilgarn Craton.||||||07-FEB-11
18604|Triumph Gabbro|60627|5|Briefly described|p65 Tb.1|||Of Black Flag Group.||||||
18604|Triumph Gabbro|62108|5|Briefly described|p1409 Tb. 8|||Thickness: ~600m. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone).||||||07-FEB-11
18604|Triumph Gabbro|65834|6|Mentioned|p7, 62|||Kambalda Domain, Kalgoorlie Terrane.||Black Flag Group.||||
18604|Triumph Gabbro|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2680 Ma (inferred).|Great Boulder Suite|||Gabbro to quartz dolerite; thin basal pyroxenite; metamorphosed.|
18604|Triumph 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.|2680 Ma (inferred)|Unit of Great Boulder Suite.|||Gabbro to quartz dolerite; thin basal pyroxenite; metamorphosed|
18604|Triumph Gabbro|72095|5|Briefly described|p10-17|||Kambalda Region, Eastern Goldfields, Yilgarn Craton. Compositionally indistinguishable from Low-Th Basalt (LTB) of Barnes et al., 2012. Detailed geochemistry is described.||||||
18604|Triumph Gabbro|73391|6|Mentioned|Appendices.|||Langsford (1989). Regional stratigraphic correlation chart of other workers.|||||Differentiated dolerite, cumulate pyroxenite, spotted gabbro, leucodolerite, granophyric quartz dolerite.|
18605|Triwhite Sandstone|7433|4|Described|p25 Fig.2, p32 Fig.8, pp36-37. |Artinskian|Artinskian|Kidson Sub-basin, Canning Basin. Shallow marine clastics. Has wavy and lenticular bedding, and low-angle cross-stratification. Lithology resembles Lightjack Formation.||||Overlies Noonkanbah Formation. Is overlain by Lake George beds.|Muscovite-rich, thin-bedded sandstone and siltstone; intraformational mud-clast conglomerate containing marine fauna.|
18605|Triwhite Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
18605|Triwhite Sandstone|35127|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35201|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35202|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35207|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35222|4|Described|Table.2|||||||||
18605|Triwhite Sandstone|35223|4|Described|Table.2|||||||||
18605|Triwhite Sandstone|35225|4|Described|Table 1|||||||||
18605|Triwhite Sandstone|35226|4|Described|Table 1|||||||||
18605|Triwhite Sandstone|35250|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35251|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35252|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|35497|4|Described|Table 1|||Also on P10||||||
18605|Triwhite Sandstone|35903|4|Described|Table 1|||||||||
18605|Triwhite Sandstone|36632|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18605|Triwhite Sandstone|36890|3|Fully described|p344|||||||||
18605|Triwhite Sandstone|38878|6|Mentioned|Map legend|Kungurian|Artinskian|Artinskian - Kungurian||||||
18605|Triwhite Sandstone|42613|6|Mentioned|P 17|||||||||
18605|Triwhite Sandstone|42734|5|Briefly described|map legend|Permian||||||||
18605|Triwhite Sandstone|43563|6|Mentioned|Fig.2,p5||Kungurian|||||||
18605|Triwhite Sandstone|43818|6|Mentioned|Fig.2.p39||Early Permian|Liveringa Group possible parent?||||||
18605|Triwhite Sandstone|44143|4|Described|p435 Table 4-19, p445, p446 Figure 4-102|Early Permian|Early Permian|Unit in Liveringa Group (although not evident in Tb. 4-19). Up to 100m thick; sandstone interbedded with siltstone and intraformational claystone and conglomerate; shallow marine. Conformably overlies Noonkanbah Formation; equivalent to part of Lightjack Formation. Type section 1.6km east of Dunn Soak (TABLETOP: 22deg 04' S, 123deg 10' E).||||||24-NOV-17
18605|Triwhite Sandstone|44357|5|Briefly described|p17||Permian|To the south.||||||
18605|Triwhite Sandstone|44994|6|Mentioned|Fig.7|||Correlation.||||||
18605|Triwhite Sandstone|44998|2|Defined|p91|Kungurian|Artinskian|Overlies Dora Shale. Correlated with Maitland Group, NSW. Kung.-u.Artinsk. On many pages. p.70,86,88,103-4,233, map.||||||
18605|Triwhite Sandstone|45153|2|Defined|App.4-79|Early Permian|Early Permian|See also App.4-73||||||
18605|Triwhite Sandstone|45158|3|Fully described|p20|||See also P13||||||
18605|Triwhite Sandstone|45168|6|Mentioned|p6|||||||||
18605|Triwhite Sandstone|66949|5|Briefly described|p26, p56 Appx.3, p82 Appx.5|Permian|Permian|Traves et al. (1956). Early Permian. Type section detailed. Up to 100m thick; shallow marine deposits.||||Correlated with lower part of Liveringa Group.|Sandstone interbedded with siltstone and intraformational claystone and conglomerate.|
18605|Triwhite Sandstone|67202|5|Briefly described|p7, p43, p44 Fig.2.10, p67-69, p281|Permian|Permian|One of the dominant aquifers in the Canning Basin; bores sunk every c.20km along Canning Stock Route. Supplies the community at Punmu; also discharges at springs around Lake Dora. Shallow-marine deposits up to 77m thick.||Liveringa Group.||Overlies the Noonkanbah Formation. Unconformably overlain by the Callawa Formation.|Fine- to medium-grained, silty, micaceous sandstone interbedded with siltstone, shale; laminated to medium bedded, cross-bedded; minor intraformational conglomerate; micaceous, trace fossils. Locally heavily indurated by calcrete.|15-FEB-18
18605|Triwhite Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||claystone, conglomerate, sandstone|
18608|Troughton Group|13194|5|Briefly described|p385 Tb. 4-16, p396 fig 4-60|Jurassic|Triassic|Up to 1500m thick.||||Overlies Sahul Group, Kinmore Group (both conformably). Part equivalent to Sahul Group.||
18608|Troughton Group|13222|6|Mentioned|p229 Fig.2.||||||Includes Cape Londonderry Formation.|||
18608|Troughton Group|13354|6|Mentioned|p375 Fig.6.|Middle Jurassic|Early Jurassic|Comprises upper Nome Formation and Plover Formation.||52||||28-OCT-14
18608|Troughton Group|22663|5|Briefly described|AC97 1-4 Fig.4||Jurassic|||||||01-MAR-10
18608|Troughton Group|24569|5|Briefly described|p248 Fig. 3|Jurassic|Triassic|Includes Cape Londonderry, Malita and Plover Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
18608|Troughton Group|41459|6|Mentioned|Fig.2|||Reserved as Troughton Formation||||||
18608|Troughton Group|41532|3|Fully described|p304|||||||||
18608|Troughton Group|41731|6|Mentioned|Fig.3|||||||||
18608|Troughton Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
18608|Troughton Group|42066|5|Briefly described|Fig.3 P199|||||||||
18608|Troughton Group|42075|5|Briefly described|Fig.4 P245|||||||||
18608|Troughton Group|42442|3|Fully described|p23|||Variation of Troughton Group, WA.||||||
18608|Troughton Group|43661|6|Mentioned|Fig.3|||||||||
18608|Troughton Group|43699|6|Mentioned|p3|Middle Jurassic|Early Jurassic|||||||
18608|Troughton Group|43707|5|Briefly described|Fig.3,p4||Jurassic|||||||
18608|Troughton Group|43739|6|Mentioned|p10|Jurassic|Triassic|||||||
18608|Troughton Group|49637|5|Briefly described|Fig.3|Middle Jurassic|Late Triassic|Includes the Malita and Plover Formations.||||||07-FEB-11
18608|Troughton Group|60634|6|Mentioned|p1168 Fig.3. |Middle Jurassic|Early Jurassic||||Includes Plover Formation.|Overlies Sahul Group. Is overlain by Swan Group.||
18608|Troughton Group|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Triassic|Includes Cape Londonderry, Malita and Plover Formations.  Age: ~240-~154Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
18608|Troughton Group|63062|5|Briefly described|p9 Fig. 9|Middle Jurassic|Early Jurassic|Included in terms of equivalents, and represented in the study area by only its youngest component, the Plover Formation. Geological Province: Arafura and Money Shoal Basins. See also pp32-33 Figs. 29 and 30.||||||07-FEB-11
18608|Troughton Group|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||Overlies Kinmore Group.||
18608|Troughton Group|68135|5|Briefly described|p51 fig 2a|Middle Jurassic|Early Jurassic|Bonaparte Basin.|||Malita, Plover Formations.|Is overlain by Flamingo Group.||15-SEP-17
18608|Troughton Group|69297|6|Mentioned|p285, p289, p290, p305, p322|Middle Jurassic|Early Jurassic|Arafura Basin.|||Includes the Plover Formation and the Ashmore Volcanics.|Overlies the Sahul Group. Overlain by the Swan Group.||
18608|Troughton Group|69451|6|Mentioned|p35:2 Fig.35.2; 35:3 Fig.35.4;|Jurassic|Jurassic|||||||12-JUL-16
18608|Troughton Group|69452|4|Described|p36:4-5, 8, 15, 19, 21|Middle Jurassic|Middle Triassic|Gunn (1988). An offshore succession extending across much of the Bonaparte Basin. Fluvial braided-stream, continental, deltaic fluvial to coastal.|||Cape Londonderry, Malita, Plover Formations; Ashmore Volcanics.|Unconformably overlies Mount Goodwin Subgroup. Is overlain by Flamingo Group disconformably to unconformably.|Dominantly siliciclastic rocks.|12-JUL-16
18608|Troughton Group|69454|5|Briefly described|p38:4|Rhaetian|Anisian|Petrel Sub-basin, Bonaparte Basin.|||Cape Londonderry, Malita Formations.|Overlies Kinmore Group.||12-JUL-16
18608|Troughton Group|69456|5|Briefly described|p40:1-4, 15 Fig.40.16|Middle Jurassic|Early Jurassic|Gunn (1988); defined in the Bonaparte Basin. The NT and offshore occurrences are consistently referred to as "Troughton Group equivalent".|||Cape Londonderry, Malita and Plover Formations.|||12-JUL-16
18608|Troughton Group|69653|6|Mentioned|p6, 8, 10, 14-15|Middle Jurassic|Early Triassic|Petrel Sub-basin. Deltaic to fluvial sediments; increasing shallow-marine influence in mid-Jurassic.|||Malita, Plover, Cape Londonderry Formations.|Overlies Kinmore Group. Is overlain unconformably by Flamingo Group.|Local redbeds.|
18608|Troughton Group|69673|5|Briefly described|p153 fig 125, p166 fig 136, p173||||||Includes Cape Londonderry Formation, Malita Formation, Plover Formation|Unconformably overlies Mount Goodwin Subgroup, disconformably overlain by Flamingo Group||
18608|Troughton Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Bathonian|Anisian|See also Regional geology: Figs.6-7. Sahul: Fig.2. Vulcan: Fig.2.|||Cape Londonderrry, Malita and Plover Formations; Ashmore Volcanics.|Overlies Kinmore Group. Is overlain by Flamingo Group.||12-JUL-16
18608|Troughton Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Bathonian|Hettangian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Plover Formation; Ashmore Volcanics.|Overlies Sahul Group. Is overlain by Swan Group.||12-JUL-16
18608|Troughton Group|70098|5|Briefly described|p3, p18 Fig.4, p19 Fig.5|Middle Jurassic|Early Jurassic|Money Shoal Basin. Shown as Flamingo Group-Troughton Group, Early Cretaceous - Jurassic.|||Plover Formation|Overlies Kulshill Group (and equivalent?).||
18668|Tumbiana Formation|22475|5|Briefly described|Fig.3, p498|Archean|Archean|Of the Fortescue Group.||||||07-NOV-08
18668|Tumbiana Formation|22717|6|Mentioned|p10|||||||||17-NOV-21
18668|Tumbiana Formation|23045|6|Mentioned|291 fig 8|||Of the Fortescue Group.||||||16-JAN-07
18668|Tumbiana Formation|23046|5|Briefly described|171|||||||||
18668|Tumbiana Formation|23570|3|Fully described|p93|Archean|Archean|Of Fortescue Group. Age: 2715+/-6 (U-Pb).  Underlain by Kylena Formation. Max. thickness: 200m. Geological Province: Hamersley Basin||||||07-NOV-08
18668|Tumbiana Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Maddina Formation; underlain by Kylena Formation.||||||07-NOV-08
18668|Tumbiana Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Maddina Formation. Geological Province Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|23585|4|Described|p16|Archean|Archean|Of Fortescue Group. Overlain by Maddina Formation; underlain by Kylena Formation. In the Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|23594|4|Described|p16|Paleoproterozoic|Archean|Of Fortescue Group. Overlain by Maddina Basalt; underlain by Kylena Basalt. Geological Province: Hamersley Basin. Max. thickness: 150 m.||||||07-NOV-08
18668|Tumbiana Formation|23598|4|Described|p13|Archean|Archean|Of Fortescue Group. Overlain by Maddina Formation; underlain by Kylena Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|23612|5|Briefly described|p840|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin||||||07-NOV-08
18668|Tumbiana Formation|23745|4|Described|p11|Archean|Archean|See also page 7 Fig 5. Of Fortescue Group. Max. thickness: 103 m.||||||07-NOV-08
18668|Tumbiana Formation|23746|4|Described|p17|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin. Max. thickness: 90 m.||||||07-NOV-08
18668|Tumbiana Formation|23755|5|Briefly described|p10|Archean|Archean|Of Fortescue Group||||||07-NOV-08
18668|Tumbiana Formation|23780|5|Briefly described|p175|Archean|Archean|Of the Fortescue Group. Overlain by Maddina Basalt.||||||07-NOV-08
18668|Tumbiana Formation|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Fortescue Group.  Age: >2.715Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.>2.715 Ga. Geological Province: Pilbara Craton. Of the Fortescue Group. Overlain by Nymerina Basalt; underlain by Kylena Basalt.||||||07-NOV-08
18668|Tumbiana Formation|24025|5|Briefly described|p14|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
18668|Tumbiana Formation|24185|5|Briefly described|P750|Archean|Archean|Of the Fortescue Group. Geological Complex: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|24352|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group. Includes the Meentheena and Mingah Members. Geological Province: Hamersley Basin||||||07-NOV-08
18668|Tumbiana Formation|24353|3|Fully described|p1, p9 Fig.5, p11 Tb.2|Archean|Archean|Of the Fortescue Group. Overlain by Maddina Formation (conformable). Age: c.2719Ma. Max Thickness: 250m. Geological Province: Hamersley Basin||||||07-NOV-08
18668|Tumbiana Formation|24531|5|Briefly described|p36|Archean|Archean|Of the Fortescue Group. Green-brown shale and pisolitic tuff overlying basal arkosic grits and conglomerates of the Fortescue Group.  Max. thickness: 4m.||||||07-NOV-08
18668|Tumbiana Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group.  Age: c.2719Ma.||||||07-NOV-08
18668|Tumbiana Formation|24533|5|Briefly described|p9, p5 Table 2|Archean|Archean|Of the Fortescue Group. Coastal and seashore facies, with clastic and volcaniclastic rocks. Overlies the Kylena Formation conformably. Age: 2719 +/- 6Ma. Max. Thickness: <200m. Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group.  Age: c.2719Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|24541|3|Fully described|p1, p11 Tb.2, p51|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2719 Ma. Conformably overlain by Maddina Formation and Jeerinah Formation. Overlies the Kylena Formation. Maximum Thickness: 200m.||||||07-NOV-08
18668|Tumbiana Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2719Ma.  Volcaniclastic sandstone, and siltstone, argillite, tuff and stromatolitic carbonate rocks; minor basalt and chert.||||||07-NOV-08
18668|Tumbiana Formation|24554|4|Described|p5, p12|||Of the Fortescue Group. Conformably overlies the Kylena Formation. Four subdivisions are recognized on WHITE SPRINGS. Where the basalt component is present, it typically underlies the Meentheena Member. Geological Province: Hamersley Basin, Pilbara Craton||||||
18668|Tumbiana Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Fortescue Group. Contains the Mingah tuff member. Age: >/=2715Ma.||||||07-FEB-11
18668|Tumbiana Formation|31307|5|Briefly described|p80|||||||||
18668|Tumbiana Formation|31853|2|Defined|p63|Archean|Archean|||||||07-NOV-08
18668|Tumbiana Formation|35641|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18668|Tumbiana Formation|36551|6|Mentioned|Table 23|||||||||
18668|Tumbiana Formation|37297|6|Mentioned|Fig.2|||||||||
18668|Tumbiana Formation|38988|6|Mentioned|p5|||||||||
18668|Tumbiana Formation|39200|6|Mentioned|p279|||||||||
18668|Tumbiana Formation|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18668|Tumbiana Formation|39426|4|Described|p11|||||||||
18668|Tumbiana Formation|39444|4|Described|p33|||||||||
18668|Tumbiana Formation|39697|4|Described|p120|||||||||
18668|Tumbiana Formation|39837|6|Mentioned|Table 1|||||||||
18668|Tumbiana Formation|40369|6|Mentioned|p15|||See also Table 1||||||
18668|Tumbiana Formation|41357|6|Mentioned|p132|||||||||
18668|Tumbiana Formation|41635|6|Mentioned|p22|||||||||
18668|Tumbiana Formation|41669|3|Fully described|p24|||||||||
18668|Tumbiana Formation|42352|5|Briefly described|p5, Fig.3 p6|||||||||
18668|Tumbiana Formation|42785|5|Briefly described|Fig.3 P264|||||||||
18668|Tumbiana Formation|43055|4|Described|p14, Table 4|||Of the Fortescue Group.||||||16-JAN-07
18668|Tumbiana Formation|43056|5|Briefly described|Map Legend|||Of the Fortescue Group.||||||16-JAN-07
18668|Tumbiana Formation|43698|6|Mentioned|p26|||||||||
18668|Tumbiana Formation|44150|6|Mentioned|p132 Fig.2-131||||2.7 Ga.|||Overlies Kylena Basalt.||
18668|Tumbiana Formation|44152|5|Briefly described|p171-172, p176 Fig.2-154, p177|||[GA place names database has no Tumbiana on it; the original spelling was Tumbinna.] Originally Tumbinna Pisolite (Noldart and Wyatt, 1982); spelling inexplicably changed to Tumbiana by de la Hunty (1963, 1964); unit downgraded to Member status (of Mount Jope Volcanics) by MacLeod and de la Hunty (1966). Mapped as Pillingini Tuff by Kriewaldt and Ryan (1967) and Williams (1968). Later re-mapping uses the name Tumbiana Formation.||Fortescue Group|||Includes characteristic abundant accretionary lapilli.|
18668|Tumbiana Formation|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
18668|Tumbiana Formation|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
18668|Tumbiana Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Carbonate rock, and tuffaceous shale, sitlstone and sandstone, and pisolitic tuff.||||||07-NOV-08
18668|Tumbiana Formation|44443|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
18668|Tumbiana Formation|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
18668|Tumbiana Formation|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
18668|Tumbiana Formation|46319|4|Described|p13|Proterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
18668|Tumbiana Formation|50131|6|Mentioned|p6 Fig. 4|||Of Fortescue Group. Geological Province: Pilbara Craton.||||||22-APR-09
18668|Tumbiana Formation|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Age: c. 2719 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin. Tuffaceous siltstone and sandstone; commonly with accretionary lapilli.||||||07-NOV-08
18668|Tumbiana Formation|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.  Age: c. 2719Ma. Includes: Meentheena Member. Overlies Kylena Formation; underlies Maddina Formation.||||||07-NOV-08
18668|Tumbiana Formation|50370|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2719 Ma||||||07-NOV-08
18668|Tumbiana Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin. In the Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|50544|4|Described|p48, p44 Fig. 8|Archean|Archean|Includes the Mingah Tuff and Meentheena Carbonate Members (lower and upper units). Conformably overlies Kyleena Formation. Max. thickness: 400m.  See also p15 Tb. 1.||||||07-NOV-08
18668|Tumbiana Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Carbonate rock, and tuffaceous shale, siltstone and sandstone; minor pisolitic tuff. Overlies Mount Roe Basalt.  Age: c.2719Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|60373|4|Described|p145 Tb. 1, p147 Fig. 2, p150 Tb. 2|Archean|Archean|Of Fortescue Group. Overlain by Maddina Formation, underlain by Kylena Formation. Age: 2724+/-5, 2727+/-5, 2721+/-4. SHRIMP ages; 2715+/-6, 2719+/-6Ma. Tuffaceous sandstone and volcaniclastic sandstone. Also on p161 Fig. 6, p162, p164.||||||18-JAN-12
18668|Tumbiana Formation|60429|4|Described|p20 Fig. 5, p21, p22|Archean|Archean|Of Fortescue Gp. Formerly Bamboo Creek Porphyry - recent studies led to revised lith.Comprises Mingah Tuff Member + Meentheena Carbonate Member. Age: 2756+/-8Ma (SHRIMP U-Pb, Arndt et al, 1991). Max. thickness:500m in Helen Well area. Detailed lithology.||||||07-FEB-11
18668|Tumbiana Formation|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
18668|Tumbiana Formation|60706|5|Briefly described|p625 Fig.3, p637 Fig.9|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
18668|Tumbiana Formation|61254|5|Briefly described|p255-273|Neoarchean|Neoarchean|Pilbara Craton. 170m thick. Called Tumbian on p257 and 260. Lithology and paleoenvironment described in detail. Outcrops as a narrow strip along the southern margin of the Pilbara Craton. Unconformably overlies Archean basement rocks. The lower part is interpreted as an alluvial fan deposit, the middle is interpreted to be a transgressive surface. The upper part is interpreted to have developed in a coastal to shallow marine environment.|2715 +/- 6 Ma (U-Pb: Arndt et al., 1991)|Of the Fortescue Group.|Includes Minger Tuff Member and Meentheena Carbonate Member.|Unconformably overlain by the Maddina Formation.|Conglomerates; then transgressive conglomerates and/or breccias passing upward into mafic tuffaceous mudstones and sandstones intercalated with volcanics; then stromatolitic carbonates with minor mudstones and sandstones.|24-APR-20
18668|Tumbiana Formation|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|61265|4|Described|p43, p51 Tb.2|Archean|Archean|Of the Fortescue Group. Locally overlies the Kylena Formation. Age: 2715+/-6 Ma (Arndt et al. 1991). Consists predominantly of volcaniclastic sandstone with minor tuff and stromatolitic carbonate rock. Geological Province: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|61266|5|Briefly described|p58 Tb.1|Archean|Archean|Of the Fortescue Group. Mingah tuff member; pisolitic and felsic tuff. Geological Province: Pilbara Craton.||||||17-NOV-21
18668|Tumbiana Formation|61268|5|Briefly described|p79, p81 Tb.1, p80 Fig.2|||Of Fortescue Gp. Conformably overlain by Maddina Fm. Composed of 3 members: lower 50m thick unit of tuff, siltstone, shale and stromatolitic carbonate rock, overlain by ~100m of vesicular basalt and andesite, and an upper 50m thick unit of pisolitic tuff.||||||
18668|Tumbiana Formation|62576|5|Briefly described|p619|Archean|Archean|Of the Fortescue Group. Age: 2720Ma. Geological province: Pilbara Craton.||||||07-NOV-08
18668|Tumbiana Formation|62579|5|Briefly described|p116|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergp). Age: 2724+/-5 and 2721+/-4Ma. Geol.Prov: Pilbara Craton. Dominantly clastic sedimentary rocks. Consists mostly of volcaniclastic rock, volcaniclastic sandstone, stromatolitic carbonate, chert, basalt and tuff.||||||07-NOV-08
18668|Tumbiana Formation|63367|4|Described|p230-234, p236, p245-246|Neoarchean|Neoarchean|Extends for over 680 km across N exposure of Fortescue Group. Various authors argue for a lacustrine setting. Trace elements and REE + Y data discussed in detail.|ca. 2725 Ma (Blake et al., 2004)|Unit in Fortescue Group.||Lateral facies equivalent to Pyradie Formation (South Pilbara).|Consists of <320m of large scale cross-stratified sandstone, complexly cross-bedded calcareous sandstone, stromatolitic and fenestrate carbonate, micaceous quartz sandstone, and volcanic tuff.|
18668|Tumbiana Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2719Ma. Underlies: Maddina Formation. Overlies: Kylena Formation. Mafic to felsic volcaniclastic sandstone, pyroclastic rocks, and fine to medium grained clastic sedimentary rock; basalt.||||||07-NOV-08
18668|Tumbiana Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Age: 2729-2716Ma. Geological Province: Fortescue Basin. Massive, basaltic volcanic rocks and carbonate rocks.||||||07-NOV-08
18668|Tumbiana Formation|64326|6|Mentioned|p73|Archean|Archean|Typically overlie Kylena Formation in the Fortsecue Group but in this instance, the rocks overlying Kylena Fm due to compositional and depositional differences, are named Pear Creek Formation.||||||17-NOV-21
18668|Tumbiana Formation|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Contains the Pillingini Tuff. Geological province: northen Pilbara Craton. Siliceous limestone (stromatolitic) and pisolitic tuff; subordinate tuff, basalt and sediments.||||||07-FEB-11
18668|Tumbiana Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Basaltic volcanic rocks and carbonate rocks.||||||09-DEC-08
18668|Tumbiana Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Mingah and Meentheena Members. Age: c. 2719Ma.  Geological Province: Pilbara Craton.||||||07-FEB-11
18668|Tumbiana Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes 2 members.  Age: 2719Ma - 2715Ma. Geological Province: Pilbara Craton (Hamersley Basin). Basaltic to andesitic volcaniclastic siltstone and sandstone; well bedded, with local cross-bedding and accretionary lapilli.||||||17-NOV-08
18668|Tumbiana Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Meentheena and Mingah Members.  Age: 2719-2715Ma. Geological Province: Hamersley Basin. Basaltic volcanic rocks and carbonate rocks.||||||
18668|Tumbiana Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Meentheena and Mingah Members.  Age: 2719-2715Ma. Geological Province: Hamersley Basin. Basaltic to andesitic volcaniclastic siltstone and sandstone; well bedded.||||||
18668|Tumbiana Formation|64724|4|Described|p43, p42 Fig. 3|Neoarchean|Neoarchean|Basalt erupted during extension of the Hamersley Basin.||Of Fortescue Group.||||02-APR-12
18668|Tumbiana Formation|65008|5|Briefly described|p7, p8 Fig.5, p15 Tb.1, p21, p23, p41|Neoarchean|Neoarchean|Hamersley Basin. Geochronology by: D.R. Nelson, 2001, GSWA Record 2001/2, p.129-132, 140-148, 175-177. ~500m thick.|ca. 2719 Ma|Of the Fortescue Group|Includes the Mingah Member and Meentheena Member.|Underlain by the Kylena Formation.||15-MAY-14
18668|Tumbiana Formation|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Includes Meentheena Member, Mingah Member and unnamed basalt. Under Maddina Fm; over Kylena Fm. Age: 2719-2715 Ma (geochronology: NT Ardnt et al 1991; TS Blake et al 2004; DR Nelson 2001). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
18668|Tumbiana Formation|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton. Also includes two un-named sub-units.|c.2719 Ma (Blake 2001).|Of Fortescue Group.|Includes Meentheena Member and Mingah Member.|Mingah Member of the Tumbiana Formation overlies Kylena Formation.|Volcaniclastic pisolitic sandstone and wacke; vesicular, amygdaloidal, and massive basalt.|19-MAR-13
18668|Tumbiana Formation|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin. Also includes two un-named sub-units.|2729 - 2715 Ma (Blake et al. 2004).|Of Fortescue Group. |Includes Meentheena Member and Mingah Member.||Basaltic to andesitic volcaniclastic siltstone and sandstone, well bedded, local cross-bedding, common welded matrix, local shale, quartz sandstone and wacke; vesicular, amygdaloidal and massive basalt.|
18668|Tumbiana Formation|65825|4|Described|p4, p7 Fig.4,  p22. |Archean|Archean|Fine-grained volcaniclastic rocks with minor carbonate (named Mingah Tuff Member by Lipple, 1975); and an upper unit of stromatolitic carbonate and calcareous sandstone (the Meentheena Carbonate Member of Lipple, 1975).|c.2724 - 2715 Ma (Blake et al. 2004).|Unit in Fortescue Group.||Conformably overlies Kylena Formation.|Fine-grained sandstone, typically basaltic in composition, intercalated with thin basalt flows; siltstone; a distinctive blue-grey or green-grey, tuffaceous sandstone or granulestone containing abundant accretionary lapilli with grain-size grading.|
18668|Tumbiana Formation|65827|3|Fully described|Tb.3 p12, p32, p33 Fig.6, p37-39|Neoarchean|Neoarchean|Of Fortescue Group. Includes Meentheena Member (formerly Meentheena Carbonate Member) and Mingah Member (formerly Mingah Tuff Member). 2727-2715 Ma. Conformably/disconformably overlies Kylena Formation; conformably underlies Maddina Formation;  shown as equivalent to Mount Jope Supersequence(1). Mafic phreatomagmatic pyroclastic and lacustrine deposits.||||||21-JAN-22
18668|Tumbiana Formation|65828|5|Briefly described|Map legend|Archean|Archean||c.2719 Ma (Nelson 2001).|Unit in Fortescue Group.||Overlies Kylena Formation. Is overlain by Maddina Formation.|Tuffaceous siltstone and sandstone; commonly with accretionary lapilli.|
18668|Tumbiana Formation|65829|4|Described|p7 Fig.3, p10, p15, pp19-20.|Neoarchean|Neoarchean|Continuously exposed over 46 km. Part of Mount Jope Supersequence (Blake et al. 2004).||Unit in Fortescue Group.|Includes Mingah and Meentheena Members.|Overlies Kylena Formation conformably or disconformably.||
18668|Tumbiana Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. 2727-2715 Ma. Basaltic volcanic rocks and carbonate rocks.||||||
18668|Tumbiana Formation|66217|5|Briefly described|p45.|||Fortescue Basin. Coastal, nearshore-shelf, and lacustrine sedimentary and volcaniclastic rocks.||Unit in Fortescue Group.||||
18668|Tumbiana Formation|66685|4|Described|p215-8, p226, p228-30, p236 |Archean|Archean|Pilbara Craton. A few meters to 320 m thick, usually ~200 m thick. Complex and varies considerably for 680 km across the craton; possible depositional diachroneity. Several age estimates ranging from 2727 +/- 5 Ma (zircon U-Pb, Blake et al., 2004) to 2715 +/- 6 Ma (Arndt et al., 1991).|2720 Ma (Bolhar and Van Kranendonk, 2007).|Fortescue Group|Meentheena Member, Mingah Member.|Locally conformably or unconformably overlies the Kylena Formation, and unconformably overlies the Hardey Formation. Generally underlies  Maddina Formation conformably .|Limestone, argillite, sandstone, siltstone, shale, tuff, rare dolostone, conglomerate, and basalt.|
18668|Tumbiana Formation|67025|6|Mentioned|p322 Table 3.|||Hamersley Basin. Mean bulk susceptibility of this and other units is discussed in this article.||||||
18668|Tumbiana Formation|67130|5|Briefly described|p1, p3 fig 2, p42, p51, p53 fig 51|Neoarchean|Neoarchean|Parts of this unit were deposited in a shallow marine (coastal) setting. Evidence of bacterial activity and nature of microfossils discussed in detail.|2727 Ma - 2715 Ma|Fortescue Group||Overlies Kylena Formation, overlain by Maddina Basalt|Carbonates (dolomite) with abundant stromatolites and sparse, poorly preserved filamentous microfossils.|
18668|Tumbiana Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Fortescue Group||||
18668|Tumbiana Formation|67201|4|Described|p28-30, p51|||Equivalent to Pyradie Formation.|2727-2715 Ma|Fortescue Group|Meentheena Member, Mingah Member|Overlies Kylena Formation apparently conformably, locally unconformably, or where absent, Hardey Formation. Is overlain by Maddina Formation apparently conformably, locally unconformably.|Quartz sandstones, fine-grained volcaniclastic sandstone, siltstone and shale, and minor stromatolitic limestone and dolostone. Pyroclastic air-fall tuff.|25-NOV-16
18668|Tumbiana Formation|67202|5|Briefly described|p51-52, p258|Archean|Archean|Fortescue Basin. 100 to 150m thick.||Fortescue Group.||Overlies Kylena Basalt. Is overlain by Maddina Formation.|Tuffaceous siltstone and minor interbedded fine-grained sandstone. Also described as basaltic volcanic rocks and carbonate rocks.|
18668|Tumbiana Formation|67229|4|Described|p1-22|Neoarchean|Neoarchean|NW Pilbara Sub-basin, Fortescue Basin. Originally the Tumbiana [Tumbinna] Pisolite of Noldart and Wyatt (1962), which was divided into several Members of the Mount Jope Volcanics by MacLeod and de la Hunty (1965). de la Hunty (1965) amalgamated three of these Members into the Pyradie Pyroclastic Member (same parent), and Kriewaldt and Ryan (1967) renamed this unit the Pillingini Tuff. This was in turn renamed as three Formations (Tumbiana Formation, Nymerina Basalt, Kuruna Siltstone) by Hickman (1983). Renowned for containing some of the world's best-preserved Archean stromatolites. Generally less than 200m thick. Various stromatolitic morphologies described in considerable detail. Probably lacustrine or playa lake environment. Stratigraphic section. U-Pb zircon age.|2715 +/- 6 Ma (Arndt et al., 1991).|Fortescue Group.|Meentheena Member.|Overlies Kylena Formation conformably, Hardey Formation unconformably. Is overlain conformably by Maddina Formation. Equivalent to Pyradie Formation.|Mainly lithic sandstone, diamictic, carbonaceous clastic sandstone, lapilli tuffaceous rocks, volcaniclastic rocks, basalt and stromatolitic carbonates.|
18668|Tumbiana Formation|67269|5|Briefly described|p20-21 Fig.19|Neoarchean|Neoarchean|Pilbara. 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).|c.2720 Ma.|Fortescue Group.||||22-JUN-20
18668|Tumbiana Formation|67888|6|Mentioned|p51|Archean|Archean||2700 Ma|Fortescue Group||||
18668|Tumbiana Formation|68035|4|Described|p291, 292, Fig 6, 293|Neoarchean|Neoarchean|Fortescue Basin. Widespread stromatolites in lacustrine carbonate units. Also microbial structures described.|2727 - 2715 Ma|Of Fortescue Group.||Overlies Kylena Formation. Overlain by Maddina Formation.|Volcaniclastic rocks and stromatolitic limestone.|
18668|Tumbiana Formation|68056|5|Briefly described|p170-171, 176-186, 188-191|Archean|Archean|Pilbara Craton. Fe, C isotope data and pyrite shapes tabulated.|2715 +/- 6 Ma.|Fortescue Group.|Meentheena, Mingah Members.|Is overlain by Maddina Formation.||
18668|Tumbiana Formation|68101|4|Described|p1, p6-7, p10|Neoarchean|Neoarchean|Pyroclastic and lacustrine deposits. Contains well-preserved stromatolites.|2727-2721 Ma (Blake et al., 2004).|Fortescue Group||Disconformably overlies Kylena Formation; is overlain by Maddina Formation.|Laterally extensive fossiliferous limestones.|
18668|Tumbiana Formation|68280|5|Briefly described|p1, p5, p37|Neoarchean|Neoarchean||2727-2715 Ma|Fortescue Group||Overlain by Maddina Formation, overlies Kylena Formation|Carbonates with abundant and diverse stromatolites. Pebble conglomerates.|
18668|Tumbiana Formation|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Ages from Arndt et al. (1991) and Blake et al. (2004).|2727-2715 Ma|Of the Fortescue Group|Includes Mingah Member.|||
18668|Tumbiana Formation|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2727-2715 Ma (Arndt et al 1991; Blake et al 2004)|Of the Fortescue Group.|Includes Mingah and Meentheena Members.||Basaltic to andesitic volcaniclastic siltstone and sandstone; well bedded, with local cross-bedding and accretionary lapilli; common welded matrix; local stromatolites; local shale, quartz sandstone, and wacke.|29-APR-14
18668|Tumbiana Formation|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Mapped as 2 unnamed sub-units. Contains local stromatolites.|2727-2715 Ma|Of the Fortescue Group. |||Felsic volcaniclastic sandstone and tuffaceous rocks, minor pebbly conglomerate and quartz arenite; basaltic to andesitic volcaniclastic siltstone and sandstone, well bedded, common welded matrix, local shale, quartz sandstone, and wacke.|05-MAY-14
18668|Tumbiana Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|Includes Meentheena Member, Mingah Member||Basaltic volcanic rocks and carbonate rocks, felsic volcaniclastic sandstone and tuffaceous rocks; minor conglomerate and quartz arenite. Vesicular, amygdaloidal and massive basalt. Basaltic to andesitic volcaniclastic siltstone and sandstone.|
18668|Tumbiana 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. 2719 Ma|Unit of Fortescue Group.|Includes Mentheena Member.||Basaltic volcanic rocks and carbonate rocks|
18668|Tumbiana Formation|69299|3|Fully described|p1,5-7,9-11,14,16-20,map,Fig.4,Tbs.1,2,3|Archean|Archean|Succession of volcaniclastic rocks containing thin units of stromatolitic carbonate rocks. An exceptionally good stratigraphic marker unit. Thickness on COOYA POOYA: 200 m.  Geol. Prov: Hamersley Basin, Pilbara Craton.|2719 +/- 6 Ma (Nelson, in prep.).|Of Fortescue Group.|Includes Meentheena Member.|Overlies Kylena Formation with angular unconformity; unconformably overlies Hardey Formation; conformably overlain by Maddina Formation; stratigraphically equivalent to Pyradie Formation.|Volcaniclastic sandstone, siltstone, basaltic and andesitic tuff and tuffaceous units, and stromatolitic limestone and dolomite.|01-JUL-14
18668|Tumbiana Formation|69301|4|Described|p17 Fig.6, p18-19, p22-23|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Sequence 3.|2.73-2.72 Ga|Fortescue Group|Meentheena Member, Mingah Member|Overlies Kylena Formation. Is overlain by Maddina Formation.|Composed of quartz sandstones, fine-grained volcaniclastic rocks, shale, and stromatolitic limestone. Lacustrine environment. Stromatolites and microbial mats (evidence of Archean life). Microbial structures within stromatolites.|
18668|Tumbiana Formation|69411|4|Described|p282-283,285-286,290-291,293,295|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Thickens from north to south, and laterally equivalent to Pyradie Formation. Outcrops along southern margin of Pilbara Craton and hosts abundant, diverse, well preserved stromatolites. U-Pb zircon dates from tuffaceous sandstones include (2715+\-6 Ma, Arndt et al., 1991; 2719+\-6 Ma, Nelson, 2001; 2721+\-4 Ma, Blake et al., 2004). Variably metamorphosed to prehnite-pumpellyite facies in the northeast, northwest and Marble Bar sub-basins, and to actinolite facies in the southern sub-basin (Smith et al., 1982). Deposition alongside an active biological methane cycle.|2.72 Ga|Unit of Fortescue Group.||Overlain by Maddina Formation. Underlain by Kylena Formation.|Volcaniclastic rocks, sandstone, siltstone, mudstone and thin, lenticular carbonate units in the NW.|
18668|Tumbiana Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
18668|Tumbiana Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Northwest Pilbara Sub-basin; 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.|2727-2715 Ma (isotopic, inferred)|Unit of Fortescue Group.|Includes Meentheena Member, Mingah Member.||Amygdaloidal basalt; massive, porphyritic, and vesicular; local pillow basalt, also vesicular basalt; basaltic to andesitic volcaniclastic siltstone and sandstone, felsic volcaniclastic sandstone and tuffaceous rocks, minor conglomerate.|
18668|Tumbiana Formation|69792|5|Briefly described|p1095-8, p1106-07||||c.2720 Ma.|Unit in Fortescue Group.|Includes Meentheena Member.|Disconformably overlies Kylena Formation.|Pyroclastic and lacustrine deposits. Includes micritic limestone members.|22-JUN-20
18668|Tumbiana Formation|69989|6|Mentioned|p33|Archean|Archean|Variations in S isotope ratios may reflect temporal changes in atmospheric chemistry.||||||
18668|Tumbiana Formation|70086|5|Briefly described|p207|Neoarchean|Neoarchean|Stromatolites contain thin, irregular patches of carbonate precipitates, interpreted as lake-floor precipitates (Flannery and Walter, 2012; Lepot et al., 2008, 2009).|2720+\-5 Ma|Unit of Fortescue Group.||||
18668|Tumbiana Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean||2735-2629 Ma|||||
18668|Tumbiana Formation|71042|5|Briefly described|p66|Archean|Archean|Oakover Basin, Southern Pilbara.||Fortescue Group||||
18668|Tumbiana Formation|71169|6|Mentioned|p64|Neoarchean|Neoarchean||2719 +/- 6 Ma (Nelson, 2001)||||Volcaniclastic sandstone.|
18668|Tumbiana Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||limestone, crystalline dolostone/dolomite, mudstone, ash tuff|
18668|Tumbiana Formation|71803|4|Described|p366, p368, p387|Neoarchean|Neoarchean|Pilbara Craton. An additional age of 2715 +/- 6 Ma is derived from Arndt et al, 1991.|2724+/- 5 Ma (Blake et al, 2004)|||Lateral equivalent to the Pyradie Formation.|Thin sequence of primarily lacustrine and near-shore sedimentary rocks ranging from stromatolitic carbonates to sandstones, conglomerates and tuffs.|
18668|Tumbiana Formation|71808|5|Briefly described|p8, p149|||Pilbara Craton. Equivalent to a felsic pyroclastic unit in the east.||Fortescue Group||Equivalent to the Pyradie Formation.|Tuffaceous sediments and biogenic dolomite.|
18668|Tumbiana 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 2727+/-5 Ma, min2715+/-6 Ma.|Fortescue Group, sequence 4|||Basaltic volcanic rocks and carbonate rocks.|
18668|Tumbiana Formation|72489|6|Mentioned|p12|Archean|Archean|||||||
18668|Tumbiana Formation|72712|6|Mentioned|p8, p10 Fig.6.|Neoarchean|Neoarchean|Commonly less than 200 m thick sedimentary rock.||Fortescue Group||Overlies Kylena Formation and underlies Maddina Formation and is equivalent to Pyradie Formation.|Includes carbonate and siliciclastic sedimentary rocks.|
18668|Tumbiana Formation|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Written as Pyradie Formation / Tumbiana Formation. Ages of 2715 +/- 6 Ma and 2724 +/- 5 Ma were reported by Mole et al. (2018) for these units.|2715 +/- 6 Ma, 2724 +/- 5 Ma|Fortescue Group||Underlain by Kylena Formation / Boongali Formation. Overlain by Maddina Formation / Bunjinah Formation.|Includes carbonates and/or mafic volcanics.|
18674|Tumblagooda Sandstone|1943|5|Briefly described|p373, p376|||Of Kalbarri Group. Upgraded herein to Tumblagooda Group.||||||
18674|Tumblagooda Sandstone|6943|5|Briefly described|pp599-600, pp602-603, pp605-606.|Earliest Silurian|Ordovician|Contains conodonts and a diverse trace fossil assemblage.|||||Red-bed sandstone succession.|
18674|Tumblagooda Sandstone|6944|6|Mentioned|p571.|Ordovician|Cambrian|Southern Carnarvon Basin. Disconformably underlies Nannyarra Formation.||||||27-OCT-14
18674|Tumblagooda Sandstone|12471|6|Mentioned|p475 Fig.2. |Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|12729|4|Described|Throughout|Silurian|Ordovician|Age estimates from Late Cambrian to Cretaceous, this ref. suggests Late Ordovician to Early Silurian. Outcrops in coastal cliffs at Shell House, south of Kalbarri. Gravity data near Woodleigh impact, indicates lateral changes in density due to deformation caused by the impact. Mis-named as Tumblagooda Formation in seismic sections Figs. 11, 16-17.||||Conformably underlies the Dirk Hartog Group, underlies the Wittecarra Sandstone.|Redbed sandstone succession.|
18674|Tumblagooda Sandstone|12731|5|Briefly described|p590 Fig.2, p594.|Late Ordovician|Late Ordovician|Thickens significantly to the south to 3500 m, suggesting change in the depocentre possibly caused by uplift along the Wandagee-Ajana Ridge in the Silurian. Minor gas shows in Wandagee 1. Potential hydrocarbon reservoir sealed by Dirk Hartog Group shales.|||||Sheet-braided, fluvial to coastal red beds.|
18674|Tumblagooda Sandstone|12733|6|Mentioned|p554 Fig.2.|Ordovician|Ordovician|Predominantly fluvial to tidal high-energy conditions.||||Overlain by Dirk Hartog Group.||
18674|Tumblagooda Sandstone|13615|3|Fully described|p2, 4, p6-8, p15-16, 33, 104 App. 3|Late Ordovician|Ordovician|Peedamullah Shelf. Up to 1000m thick. Overlain by Devonian clastic and carbonate rocks. The type section occurs in the Murchison River from the Hardabut Fault to Second Gully; 27deg52'40" S 114deg33'30'E to 27deg37'20"S 114deg12'10"E. Deposited in a braided fluvial or mixed fluvial and eolian sandsheet. See also p118, Plates 2,3.||||Unconformably overlain by the Nannyarra Sandstone.|Red sandstone and conglomerate, very minor siltstone and mudstone.|11-FEB-19
18674|Tumblagooda Sandstone|13995|5|Briefly described|p103|Late Ordovician|Late Ordovician|Carnarvon Basin. Age inferred from Early Silurian age of overlying unit. A variety of marginal to nonmarine (terrestrial) coastal depositional environments. Has a richly diverse assemblage of arthropod trackways, some thoguht to be eurypterids, and some of large (up to 300mm wide) size.||||Is overlain by Ajana Formation.||
18674|Tumblagooda Sandstone|14227|5|Briefly described|p3, Enclos.2|Ordovician|Ordovician|Underlies Dirk Hartog Formation. Thick basal clastics in the basin. Geological province: South Carnarvon Basin.||||||07-FEB-11
18674|Tumblagooda Sandstone|14228|4|Described|p4, p5 fig2, p6 fig3, p13-14, p18-21 |Late Ordovician|Late Ordovician|Clarke and Teichert (1948). It is possible this unit is Cambrian, but probably Ordovician. 2000m to 3500m thick. Gascoyne Platform. A subartesian aquifer in southern onshore Gascoyne Platform.||||Overlain by Wittecarra Sandstone or Ajana Formation.|Redbed sandstone facies with rare siltstone and mudstone.|
18674|Tumblagooda Sandstone|22814|5|Briefly described|fig2|Silurian|Silurian|||||||
18674|Tumblagooda Sandstone|23279|5|Briefly described|p2||Silurian|(Hocking, 1991).||||||
18674|Tumblagooda Sandstone|23292|14|Not recorded|4|||||||||
18674|Tumblagooda Sandstone|23403|5|Briefly described|p4|Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|23520|5|Briefly described|p6 Fig. 4|Silurian|Ordovician|Max. thickness: >500m.  Geological Province: Abrolhos Sub-basin.  See also p3.||||||
18674|Tumblagooda Sandstone|23572|4|Described|p7, 10|Late Ordovician|Middle Ordovician|Geological Province: Carnarvon Basin. Overlying Unit: Dirk Hartog Group and Kockatea Shale. Max. thickness: ~3500m.||||||
18674|Tumblagooda Sandstone|23726|5|Briefly described|p13|Ordovician|Ordovician|Overlying Wittecarra sandstone.||||||
18674|Tumblagooda Sandstone|23815|4|Described|p272|Silurian|Late Ordovician|Geological Province: Carnarvon Basin. Overlying units: Dirk Hartog Formation (conformable) and Gneudna Formation (unconformable). Max. thickness: >3000 m.||||||
18674|Tumblagooda Sandstone|23816|4|Described|p228|Silurian|Late Ordovician|Geological Province: Carnarvon Basin. Max. thickness: >3000 m. Overlying unit: Dirk Hartog Formation (conformable).||||||27-APR-05
18674|Tumblagooda Sandstone|23935|5|Briefly described|p11 Fig.7|Ashgill|Caradoc|Conformably overlain by Dirk Hartog Group. Geological Province: Southern Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|24058|5|Briefly described|p111|Silurian|Ordovician|Geological Basin: Perth Basin.||||||
18674|Tumblagooda Sandstone|24059|5|Briefly described|p145|Silurian|Silurian|Geological Province: Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|24160|5|Briefly described|p92|Ordovician|Ordovician|Perth Basin. Thickness >3000m.|||||Red, yellow, brown to white, very fine to coarse grained, commonly conglomeratic sandstone.|
18674|Tumblagooda Sandstone|24334|5|Briefly described|p48 Tb.1|Ordovician|Late Cambrian|Age: 495-443 Ma.||||||20-DEC-06
18674|Tumblagooda Sandstone|24351|5|Briefly described|Plate 3 (in pocket)|Llandoverian|Llandoverian|Log Edel-1.||||||13-DEC-07
18674|Tumblagooda Sandstone|24390|5|Briefly described|p19 Fig. 10|Silurian|Ordovician|Geological Province: Southern Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|24410|5|Briefly described|p38, p136|Silurian|Ordovician|Variably coloured through red, yellow, brown and white.; very fine- to coarse-grained and commonly conglomeratic. Max. thickness: >3000m. See also p132.||||||24-NOV-09
18674|Tumblagooda Sandstone|24443|5|Briefly described|p19, Fig.30|Early Paleozoic|Early Paleozoic|Geological Province: Southern Carnarvon Basin. Overlies Precambrian basement.||||||07-NOV-08
18674|Tumblagooda Sandstone|24581|5|Briefly described|p811, p818|Early Silurian|Late Ordovician|||||||
18674|Tumblagooda Sandstone|29474|6|Mentioned|p9|||||||||
18674|Tumblagooda Sandstone|29548|6|Mentioned|p228|||L.Silurian - U.Ordovician||||||
18674|Tumblagooda Sandstone|29549|6|Mentioned|p144|||||||||
18674|Tumblagooda Sandstone|29591|6|Mentioned|p106|||||||||
18674|Tumblagooda Sandstone|29721|6|Mentioned|Table 226|||||||||
18674|Tumblagooda Sandstone|30186|6|Mentioned|p104|||Refers McWhae et al(1958)||||||
18674|Tumblagooda Sandstone|30875|6|Mentioned|p10|||Silurian-Devonian age||||||
18674|Tumblagooda Sandstone|30948|6|Mentioned|Map legend|Silurian|Silurian|Prob. Silurian||||||
18674|Tumblagooda Sandstone|31051|6|Mentioned|p.78.|||||||||
18674|Tumblagooda Sandstone|31561|4|Described|p31|||See also P18, 32, 34, map P24||||||
18674|Tumblagooda Sandstone|31562|5|Briefly described|p9|||||||||
18674|Tumblagooda Sandstone|31568|5|Briefly described|p17|||See also P19. Ord.-Sil.||||||
18674|Tumblagooda Sandstone|31910|4|Described|p7|||||||||
18674|Tumblagooda Sandstone|32648|6|Mentioned|p32|||Ord.-Sil.||||||
18674|Tumblagooda Sandstone|32649|4|Described|p17|||See also Table 1||||||
18674|Tumblagooda Sandstone|32714|6|Mentioned|Fig.2|||||||||
18674|Tumblagooda Sandstone|33022|6|Mentioned|Fig.2|||||||||
18674|Tumblagooda Sandstone|33044|6|Mentioned|p33|||||||||
18674|Tumblagooda Sandstone|33168|6|Mentioned|p117|||||||||
18674|Tumblagooda Sandstone|33386|6|Mentioned|Fig.7|||||||||
18674|Tumblagooda Sandstone|33453|5|Briefly described|p69|||Silurian.||||||
18674|Tumblagooda Sandstone|33622|6|Mentioned|p89|||||||||
18674|Tumblagooda Sandstone|33625|6|Mentioned|p185|||||||||
18674|Tumblagooda Sandstone|34008|6|Mentioned|p75|||L.Palaeozoic||||||
18674|Tumblagooda Sandstone|34287|6|Mentioned|p74|||||||||
18674|Tumblagooda Sandstone|34841|6|Mentioned|Fig.2|||||||||
18674|Tumblagooda Sandstone|35088|6|Mentioned|Fig.8|||||||||
18674|Tumblagooda Sandstone|35282|6|Mentioned|p1|||||||||
18674|Tumblagooda Sandstone|35653|6|Mentioned|Fig.3|||Stratigraphy of Dandaragan Trough.||||||
18674|Tumblagooda Sandstone|35971|4|Described|p84|||||||||
18674|Tumblagooda Sandstone|36199|6|Mentioned|p2|||||||||
18674|Tumblagooda Sandstone|36257|6|Mentioned|Table 2.1|||||||||
18674|Tumblagooda Sandstone|36293|2|Defined|p78|Silurian|Silurian|Prob. Silurian||||||
18674|Tumblagooda Sandstone|36890|3|Fully described|p229|||||||||
18674|Tumblagooda Sandstone|36892|5|Briefly described|p452|||||||||
18674|Tumblagooda Sandstone|37727|4|Described|p90|||See also p3.||||||11-FEB-19
18674|Tumblagooda Sandstone|37818|6|Mentioned|Table 2|||||||||
18674|Tumblagooda Sandstone|37915|6|Mentioned|p459|||||||||
18674|Tumblagooda Sandstone|38485|4|Described|p9|||See also Table 1.||||||
18674|Tumblagooda Sandstone|38771|4|Described|p53|||||||||
18674|Tumblagooda Sandstone|38998|4|Described|p15|||See also P20.||||||
18674|Tumblagooda Sandstone|39170|6|Mentioned|Fig.49|||||||||
18674|Tumblagooda Sandstone|40010|5|Briefly described|p44|||||||||
18674|Tumblagooda Sandstone|40254|6|Mentioned|p285|||||||||
18674|Tumblagooda Sandstone|40340|5|Briefly described|p8|||||||||
18674|Tumblagooda Sandstone|40341|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
18674|Tumblagooda Sandstone|40343|5|Briefly described|p10|||||||||
18674|Tumblagooda Sandstone|40617|6|Mentioned|p1|||||||||
18674|Tumblagooda Sandstone|40992|6|Mentioned|p11|||Mention Fig.5||||||
18674|Tumblagooda Sandstone|41172|4|Described|p116|||||||||
18674|Tumblagooda Sandstone|41195|6|Mentioned|Fig.2|||||||||
18674|Tumblagooda Sandstone|41271|3|Fully described|p27|||||||||
18674|Tumblagooda Sandstone|41438|6|Mentioned|p98|||See also P113||||||
18674|Tumblagooda Sandstone|41441|5|Briefly described|p151|||||||||
18674|Tumblagooda Sandstone|41443|5|Briefly described|p159|||||||||
18674|Tumblagooda Sandstone|41729|6|Mentioned|p453|||See also P454||||||
18674|Tumblagooda Sandstone|42116|4|Described|p9|||See also Fig.1||||||
18674|Tumblagooda Sandstone|42141|6|Mentioned|Table 2 P571|||||||||
18674|Tumblagooda Sandstone|42220|4|Described|p381|||See also Fig.1||||||
18674|Tumblagooda Sandstone|42393|5|Briefly described|Fig. 2 P103|||||||||
18674|Tumblagooda Sandstone|42441|1|Redefined|p1-127|Silurian|Silurian|||||||
18674|Tumblagooda Sandstone|42477|5|Briefly described|p34|||See also P88||||||
18674|Tumblagooda Sandstone|42547|5|Briefly described|p105|||Silurian.||||||
18674|Tumblagooda Sandstone|42687|6|Mentioned|map legend|||||||||
18674|Tumblagooda Sandstone|42688|6|Mentioned|map legend|||||||||
18674|Tumblagooda Sandstone|42715|4|Described|p1014|||||||||
18674|Tumblagooda Sandstone|42734|5|Briefly described|map legend|Silurian||||||||
18674|Tumblagooda Sandstone|42821|5|Briefly described|p79|||||||||
18674|Tumblagooda Sandstone|43011|6|Mentioned|Table 2,p12|||||||||
18674|Tumblagooda Sandstone|43031|4|Described|p11,Fig.2.|||||||||
18674|Tumblagooda Sandstone|43096|5|Briefly described|p6|||||||||
18674|Tumblagooda Sandstone|43566|6|Mentioned|Fig.2,p415|||||||||
18674|Tumblagooda Sandstone|43705|6|Mentioned|p11||Silurian|||||||
18674|Tumblagooda Sandstone|44144|4|Described|p500, p508 Tb.4-21, p511, p522|Silurian|Silurian|Oldest Phanerozoic rocks in Perth Basin. Type Section: Murchison River; 27o52'00''S 114o33'30''E to 27o36'30"S 114o08'30''E (Carnarvon Basin). 1000 m thick fluvial and intertidal deposits.||||Overlain unconformably by Nangetty Formation.|Red, yellow, brown, white, very fine- to coarse-grained sandstone; commonly conglomeratic.|
18674|Tumblagooda Sandstone|44532|14|Not recorded|p.5|||(G50-5).||||||
18674|Tumblagooda Sandstone|45015|2|Defined|p24-32, map legend|Paleoproterozoic|Paleoproterozoic|Quartz sandstone with minor siltstone and conglomerate. Unconformably underlies Nannyarra Greywacke; also unconformably overlain in places by Birdrong Formation. Max. thickness (est.):20,600ft.  Geological Province: Carnarvon Basin.||||||07-NOV-08
18674|Tumblagooda Sandstone|45016|14|Not recorded|p66 (map)|||||||||
18674|Tumblagooda Sandstone|45168|6|Mentioned|p6|||||||||
18674|Tumblagooda Sandstone|45965|14|Not recorded|p62|||||||||
18674|Tumblagooda Sandstone|48610|4|Described|p4,14|||(F50-13).||||||
18674|Tumblagooda Sandstone|48615|14|Not recorded|Fig.4|||||||||
18674|Tumblagooda Sandstone|48628|14|Not recorded|p1,4,6|Silurian|Ordovician|(F50-13/Wandagee). Figs.2,5. Age: Ordovician or Silurian?||||||
18674|Tumblagooda Sandstone|48823|5|Briefly described|p24|||||||||
18674|Tumblagooda Sandstone|49942|4|Described|p4 Fig.3, p7|Ashgill|Caradoc|Overlain by Ajana Formation of Dirk Hartog Group. Thickness: ~3500 m. Geological Province: Gascoyne Platform.||||||
18674|Tumblagooda Sandstone|50084|4|Described|p77|Ordovician|Ordovician|Fluvial to coastal red beds. Coarse grained sandstone with minor mudstone. Thickness: 3500 m. Overlain by Dirk Hartog Group. Geological Province: Southern Carnarvon Basin.||||||07-FEB-11
18674|Tumblagooda Sandstone|50085|5|Briefly described|p19 Fig. 10, p20 Tb. 5|Silurian|Ordovician|Geological Province: Southern Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|50621|5|Briefly described|p165 Fig. 6|Ordovician|Ordovician|Geological Province: Perth Basin.||||||
18674|Tumblagooda Sandstone|60333|6|Mentioned|p801|Late Silurian|Late Silurian|||||||
18674|Tumblagooda Sandstone|60376|5|Briefly described|p17 Fig. 4.|Silurian|Late Ordovician|Geological Province: Perth Basin. Unconformable contacts above and below the unit.||||||07-FEB-11
18674|Tumblagooda Sandstone|60384|5|Briefly described|p243 Fig 2a, p244, 250, 257, p260 |Late Ordovician|Late Ordovician|Perth and Southern Carnarvon Basins. Age shown as Caradoc to Ashgill. Trace gas at top. Braided fluvial to coastal environment.|||||Sandy redbeds|
18674|Tumblagooda Sandstone|60419|5|Briefly described|p43|Late Ordovician|Late Ordovician|Geological Province: Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|60725|5|Briefly described|p28; p29 Fig.2; p33; p35-36 Figs.5,6.|Upper Ordovician|Middle Ordovician|Good petroleum reservoir potential.||||Is overlain by Dirk Hartog Group.|Red beds.|10-MAY-17
18674|Tumblagooda Sandstone|61023|5|Briefly described|p34 Fig. 14|Silurian|Ordovician|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
18674|Tumblagooda Sandstone|61546|6|Mentioned|p385 Fig.5.|||||||||
18674|Tumblagooda Sandstone|61562|5|Briefly described|p548 Fig. 3|Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|61563|5|Briefly described|p578 Fig. 2|Ordovician|Ordovician|See also p579 Fig. 3, p582 Fig.8||||||27-JAN-06
18674|Tumblagooda Sandstone|61811|4|Described|p3 Fig.2, p7, pp8-13, p23, p26, p65.|Ordovician|Ordovician|Northern Perth Basin. Redbeds deposited in braided fluvial, tidal sandflat and coastal redbed settings. Type section along Murchison River gorge, Kalbarri National Park, where it is 1300 m thick. Type section details in Appendix 1.|||Includes the Gabba Gabba Member.|Is overlain disconformably by Wittecarra Sandstone.|Fine- to medium-grained sandstones; red,commonly bioturbated siltstone towards the top of the unit.|
18674|Tumblagooda Sandstone|61958|5|Briefly described|Map sheet 1|Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|64580|4|Described|map legend||Ordovician|Fine- to coarse-grained red-bed sandstone; minor siltstone and conglomerate.||||||09-DEC-08
18674|Tumblagooda Sandstone|64635|5|Briefly described|p4 Fig.3, p6-18      |Ordovician|Ordovician|Gascoyne Platform. p8-13, diagrams and photos of the type section in Murchison River gorge; 1300m thick. Maximum age (Arenig) from eurypterid trackways. Source of sediments for overlying Wittecarra Sandstone.|||Includes Gabba Gabba Member.|Disconformably overlain by the Wittecarra Sandstone.|Redbed deposition.|
18674|Tumblagooda Sandstone|64769|5|Briefly described|p38, p129 Fig. 132, p129|Silurian|Silurian|Geological Province: Carnarvon Basin. Slightly friable sandstone, varies from white to pink, cream and buff. Feldspathic sandstone.||||||
18674|Tumblagooda Sandstone|64972|6|Mentioned|p614, p617 Fig. 5|Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|65313|4|Described|p577-9, p580 Fig. 8, p574 Fig. 3|Silurian|Cambrian|Discussion on age constraints. See overlying Marron Member (Ajana Formation), Gabba Gabba Member, informal ?Cambrian "Tumblagooda Sandstone".  Inferred 'lower sandstone' unit dated as late Cambrian in Wandagee 1 well (p579).||||Underlies Dirk Hartog Group.||26-MAR-12
18674|Tumblagooda Sandstone|65449|5|Briefly described|p34|Ordovician|Ordovician|Southern Carnarvon Basin. Deposited in braided fluvial to high-energy coastal setings. Appears to correlate in age, at least in part, with the Carribuddy Group.||||Is overlain ?conformably by Ajana Formation (Dirk Hartog Group).|Coarse clastics.|
18674|Tumblagooda Sandstone|66589|6|Mentioned|p178, 188|Late Ordovician|Late Ordovician|Case studies cited; not visited in the field by the authors of this study. Trace fossils record marine incursions in transitional fluvial environments.||||||
18674|Tumblagooda Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark brown/red siltstone beds (10%); pale pink to pink-red medium-grained to granule sandstone (90%); predom. quartz and orthoclase.|
18674|Tumblagooda Sandstone|67200|5|Briefly described|p7 fig 5, p19 table 1|Ordovician|Ordovician|Thermal conductivity of 3.57 W/mK. See also p46, p52, p64, app 2 p4.||||Overlain by Dirk Hartog Sandstone|Sandstone with parallel and trough cross beds. Medium grained-granule sandstone with predominantly quartz and orthoclase grains; siltstone beds.|
18674|Tumblagooda Sandstone|67340|6|Mentioned|p6|Ordovician|Ordovician|Northern Perth Basin.||||||
18674|Tumblagooda Sandstone|67581|6|Mentioned|p39|Ordovician|Ordovician|||||||
18674|Tumblagooda Sandstone|67925|5|Briefly described|Ch4 p8 fig 2|Silurian|Silurian|Northern and central Perth Basin.||||Unconformably overlain by the Nangetty Formation.||
18674|Tumblagooda Sandstone|69029|6|Mentioned|p326,328|Ordovician|Ordovician|Of onshore Carnarvon Basin.||||Overlain by Dirk Hartog Group.||
18674|Tumblagooda Sandstone|69182|4|Described|Ch2 p3, Ch2 p9, Ch2 p45, Ch3 p30|Ordovician|Ordovician|Perth and Carnarvon Basins. Deposited in a braided, fluvial to coastal setting. Thickness ranging from 2000m to 3500m. See also Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110, Ch3 p3, Ch3 p8, Ch3 p11, Ch3 p23, Ch3 p35, Ch3 p67-p68, Ch3 p73.||||Conformably (or disconformably) overlain by the Dirk Hartog Group.|Red-bed sandstones with rare siltstone and mudstone.|
18674|Tumblagooda Sandstone|69297|6|Mentioned|p201, p246, p249, p250|Ordovician|Cambrian|Gascoyne Sub-Basin of the Carnarvon Basin and Perth Basin. May be in excess of 4km thick. Good potential reservoir unit.||||Overlain by the Ajana Formation, Dirk Hartog Group.||
18674|Tumblagooda Sandstone|69558|6|Mentioned|p3, p95, p96, p255-p257|Ordovician|Ordovician|Well exposed in the valley of the Murchison river.||||||
18674|Tumblagooda Sandstone|69583|5|Briefly described|p130, p131 Fig.2, p133, p134 Fig.3, p135|Ordovician|Ordovician|See also p138-139, p141-142, p152; Plates 2, 3, 4. Southern Carnarvon Basin. Seismic interpretation.||||Overlies Badgeradda Group.|Sandstone; minor siltstone and granule to pebble conglomerate.|
18674|Tumblagooda Sandstone|70375|4|Described|p817-829|Early Silurian|Late Ordovician|Condon (1965). Type section near Hardabut Pool. Southern Carnarvon Basin. Up to 2000m thick. Contains no age-diagnostic fossils. Age constrained by low-diversity conodont assemblages in the overlying Dirk Hartog Group. Divided into four facies associations: alluvial fan, braided-fluvial, tidal, near-shore marine.Zircon, tourmaline and rutile are present in small amounts.Heavy mineral assemblages support provenance from continental blocks (Yilgarn, Pilbara or East Africa/Antarctica).||||Underlies Dirk Hartog Group. Is faulted against the Northampton Complex.|Very fine-very coarse grained, rounded-subrounded and angular-subangular, moderate-well sorted pebbly red bed (quartz arenites and subarkose) showing bioturbation. Lithic grains of quartzite and chert with granite clasts.|27-SEP-16
18674|Tumblagooda Sandstone|70772|5|Briefly described|p11|Silurian|Silurian|Outcrops around Kalbarri in Western Australia. Deposited in a coastal fluvial-type setting.|||||Partially bioturbated, inter-bedded sandstone and siltstone and sections of coarse sand and conglomerate.|
18674|Tumblagooda Sandstone|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Southern Carnarvon Basin.||||||
18674|Tumblagooda Sandstone|71146|5|Briefly described|p6, p13, p14 fig 9, p26, p28|Late Ordovician|Silurian|Southern Carnarvon Basin. Oceanic depositional connections derived on the basis of rich ichnofauna. Outcrops along the Murchison River gorge and in coastal cliffs in Kalbarri National Park. Hosts diverse trace-fossil assemblages including burrows, trails, scratch marks and tunnels.||||Overlain by the Ajana Formation.|Sandy red beds.|
18674|Tumblagooda Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sandstone|
18674|Tumblagooda Sandstone|71618|6|Mentioned|p131|||Of southern Carnarvon Basin. Depositional environment: fluvial-paralic.||||||
18674|Tumblagooda Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Silurian|Ordovician|Gascoyne Platform, Southern Carnarvon Basin. Age inferred.|||||Sandstone, minor siltstone and granule to pebble conglomerate.|
18674|Tumblagooda Sandstone|72258|5|Briefly described|p127-130,133,137-138|Silurian|Ordovician|Of Perth Basin. Deposited during initiation of rifting of eastern Gondwana by at least Middle Paleozoic, along the eastern margin of Pinjarra Orogen (Halpin et al., 2017). Contains detrital zircons derived from Pinjarra Orogen and Yilgarn Craton (Cawood and Nemchin, 2000; Markwitz et al., 2017c). Major peak in Mesoproterozoic (1300-1100 Ma) and 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). 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).||||||15-JAN-20
18674|Tumblagooda Sandstone|72910|6|Mentioned|p19.|Silurian|Silurian|Drilling of the WAPET well 'Quail 1' in 1963-64, to investigate hydrocarbon potential, was terminated at 3580m in this sandstone.||||||
18674|Tumblagooda Sandstone|73346|6|Mentioned|p19|||Southern Carnarvon Basin. Includes arthropod traces.||||||
18674|Tumblagooda Sandstone|73484|5|Briefly described|p475, p476 Fig.3, p477-478, p485, p489|Paleozoic|Paleozoic|Perth Basin. Fluvio-deltaic. Loosely defined as late Silurian. See also p480-481, p484 Fig.7, p487 Fig.10.|||||Includes medium-grained sandstone with granules to pebbles of quartz, trough cross-beds.|
18692|Tunganary Formation|22547|4|Described|p21||Orosirian|Of the Speewah Group. Geological province: Speewah Basin. Thickness: 290 m. Overlies O'Donnell Formation. Overlain by Valentine Siltstone.||||||21-JUL-15
18692|Tunganary Formation|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
18692|Tunganary Formation|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Speewah Group.||||||
18692|Tunganary Formation|23751|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 280 m.||||||07-NOV-08
18692|Tunganary Formation|30097|6|Mentioned|Table 23|||||||||
18692|Tunganary Formation|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18692|Tunganary Formation|30533|5|Briefly described|p15|||On Table 2||||||
18692|Tunganary Formation|30894|5|Briefly described|p250|||Carpentarian||||||
18692|Tunganary Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18692|Tunganary Formation|30896|4|Described|p16|||||||||
18692|Tunganary Formation|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18692|Tunganary Formation|32660|5|Briefly described|Table 3|||||||||
18692|Tunganary Formation|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
18692|Tunganary Formation|32728|5|Briefly described|p34|||Mention Table 5||||||
18692|Tunganary Formation|36551|6|Mentioned|Table 10|||||||||
18692|Tunganary Formation|36885|4|Described|p186|||||||||
18692|Tunganary Formation|37462|6|Mentioned|Fig.4.9|||||||||
18692|Tunganary Formation|41987|5|Briefly described|Fig.4 P74|||||||||
18692|Tunganary Formation|42149|6|Mentioned|Table 1 P709|||||||||
18692|Tunganary Formation|42710|5|Briefly described|map legend|Proterozoic||||||||
18692|Tunganary Formation|42811|5|Briefly described|p21|||of Speewah Group||||||
18692|Tunganary Formation|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
18692|Tunganary Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
18692|Tunganary Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
18692|Tunganary Formation|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
18692|Tunganary Formation|44140|5|Briefly described|p295, p297 fig 4-4|Paleoproterozoic|Paleoproterozoic|80-360m thick.||Speewah Group|||Feldspathic and quartz sandstone, arkose, granule sandstone, green siltstone, micaceous sandstone; cross-beds, ripple marks; current scours in sandstones; graded bedding in siltstones.|
18692|Tunganary Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
18692|Tunganary Formation|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group. Buff to pale grey feldspathic sandstone, siltstone, shale, and quartz sandstone. Age: c.1835Ma. Geological Province: Speewah Basin.||||||07-NOV-08
18692|Tunganary Formation|44317|4|Described|Table 2||Carpentarian|||||||
18692|Tunganary Formation|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
18692|Tunganary Formation|44363|5|Briefly described|p.6,11,12,13,16|||(Carpentarian), Speewah Group.||||||
18692|Tunganary Formation|44364|14|Not recorded|map legend|||||||||
18692|Tunganary Formation|44366|14|Not recorded|p.11, Table 1||Carpentarian|Part of Speewah Group.||||||
18692|Tunganary Formation|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Speewah Group.||||||
18692|Tunganary Formation|44397|14|Not recorded|p.17, Table 2||Carpentarian|Speewah Group.||||||
18692|Tunganary Formation|44398|14|Not recorded|map legend||Carpentarian|||||||
18692|Tunganary Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
18692|Tunganary Formation|45047|5|Briefly described|p28|||||||||
18692|Tunganary Formation|48931|3|Fully described|p48|||||||||
18692|Tunganary Formation|60714|6|Mentioned|p113 Fig.2. |||||Of the Speewah Group.||Overlies O'Donnell Formation. Is overlain by Valentine Siltstone.||
18692|Tunganary Formation|64748|5|Briefly described|p269 Fig 2|||Of the Speewah Group; underlies the Valentine Siltstone; overlies O'Donnell Formation;||||||
18692|Tunganary Formation|67563|6|Mentioned|p122 Fig.2|||||Of the Speewah Group.||||20-JAN-17
18692|Tunganary Formation|68078|5|Briefly described|p6 figure 3, p8, p9, p14 figure 10|Paleoproterozoic|Paleoproterozoic|||Speewah Group||Overlies O'Donnell Formation, overlain by Luman Siltstone|Granophyre.|
18692|Tunganary Formation|68992|6|Mentioned|p498 Fig.1, p499|||Speewah Basin.||Of the Speewah Group.||||
18692|Tunganary Formation|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|||Speewah Group.||Overlies O'Donnell Formation. Is overlain by Valentine Siltstone.||
18692|Tunganary Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin||Speewah Group|||Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone|21-JUL-15
18692|Tunganary Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Speewah Group|||Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone.|
18692|Tunganary Formation|69585|4|Described|p4-5, p7, p9, p12-14|Orosirian|Orosirian|Western Lamboo Province. Fluvial, possibly braided, deposits. U-Pb and Lu-Hf isotope data and diagram.|1839 +/- 4 Ma (maximum depositional age).|Speewah Group.||Conformably overlies O'Donnell Formation. Is overlain conformably by Valentine Siltstone.|Poorly to moderately sorted, feldspathic or lithic-quartz sandstone with interbeds of quartz arenite, pebbly lithic sandstone, and siltstone. The upper informal member has prominent ripples.|
18692|Tunganary Formation|69634|4|Described|GEOL_LUT_CSV files|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 100k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1850-1835 Ma (Inferred)|Unit of Speewah Group.|||Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone|
18692|Tunganary Formation|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.||Unit in Speewah Group.|||Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone.|
18692|Tunganary Formation|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.||Speewah Group.||Overlies O'Donnell Formation. Is overlain by Valentine Siltstone.|Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone.|
18692|Tunganary Formation|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||1797-1835 Ma|Speewah Group|||Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone.|
18692|Tunganary Formation|70812|5|Briefly described|p6|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1850-1800 Ma|Speewah Group||||
18692|Tunganary Formation|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1850-1800 Ma|||Overlies the Valentine Sandstone. Overlain by the Luman Sandstone.|Sedimentary rocks.|
18692|Tunganary Formation|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 Valentine Siltstone. Underlain conformably by O'Donnell Formation.|Fine grained feldspathic sandstone interbedded with micaceous or sericitic siltstone, phyllite and minor coarse quartz sandstone|
18692|Tunganary Formation|71281|4|Described|p421-427, p430-432|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Speewah Basin. Up to 290m thick. Fluvial to lacustrine deposits. Photomicrographs. Zircon analyses detailed. Youngest age is 1803 +/- 12 Ma; possibly from the Sally Downs Supersuite; tectonic implications discussed.|1814 +/- 10 Ma (SHRIMP zircon).|Speewah Group.||Overlies O'Donnell Formation. Is overlain conformably by Valentine Siltstone.|Fine-grained feldspathic sandstone interbedded with micaceous or sericitic siltstone, phyllite and minor coarse quartz sandstone.|
18692|Tunganary Formation|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.||Overlies and is overlain by Hart Dolerite.|Buff and grey feldspathic sandstone, quartz sandstone, brown and green siltstone and mudstone.|
18692|Tunganary Formation|72490|5|Briefly described|p3, p5-6, p10|||Maximum thickness of 290 m. Youngest detrital zircon age component at 1814 +/- 10 Ma includes a youngest zircon at 1803 +/- 12 Ma.||Speewah Group|||Fine-grained feldspathic sandstone interbedded with micaceous or sericitic siltstone, phyllite and minor coarse quartz sandstone.|
18696|Tunney Member|23359|5|Briefly described|79|||of Muderong Shale||||||
18696|Tunney Member|23379|4|Described|p160 Fig.2;p158,159,162,163,167-174||Valanginian|of Muderong Shale, Barrow Sub-basin, Carnarvon Basin.||||||
18696|Tunney Member|24205|5|Briefly described|p242|||Of the Muderong Shale.  Geological Province: Northern Carnarvon Basin.||||||
18696|Tunney Member|37689|6|Mentioned|p24|||||||||
18696|Tunney Member|41271|6|Mentioned|p218|||||||||
18696|Tunney Member|41440|5|Briefly described|p138|||||||||
18696|Tunney Member|41446|6|Mentioned|Fig.2|||||||||
18696|Tunney Member|41732|5|Briefly described|p540|||||||||
18696|Tunney Member|42598|4|Described|P 98|late Valanginian|middle Valanginian|Invalid name - named after John Tunney, naturalist.||||||
18696|Tunney Member|63950|5|Briefly described|p336 Fig. 4|Hauterivian|Hauterivian|Of the Muderong Shale. Overlies Mardie Greensand. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
18696|Tunney Member|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||Muderong Shale.||||
18696|Tunney Member|69692|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||Muderong Formation.||||
18702|Turee Creek Group|22475|6|Mentioned|Fig.1|||||||||
18702|Turee Creek Group|22689|6|Mentioned|137|||Geological  province: Hamersley Basin. Of the Mount Bruce Supergroup.||||||16-JAN-07
18702|Turee Creek Group|22715|6|Mentioned|fig7p212|||Coupled with Hamersley Group on map legend.||||||
18702|Turee Creek Group|22716|5|Briefly described|table4 p227|Paleoproterozoic|Archean|||||||07-NOV-08
18702|Turee Creek Group|23045|5|Briefly described|289|||Age: 2449 +/-3 Ma.  Max thickness: 5000 m.||||||16-JAN-07
18702|Turee Creek Group|23046|5|Briefly described|177|||Underlain by Boolgeeda Iron Formation.||||||16-JAN-07
18702|Turee Creek Group|23047|5|Briefly described|34|||In the Hamersley Province. Of the Mount Bruce Supergroup. Overlain by Wyloo Group. See also p 41.||||||16-JAN-07
18702|Turee Creek Group|23280|6|Mentioned|p1084,Fig1p1085|||||||||
18702|Turee Creek Group|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Mount Bruce Supergroup.||||||
18702|Turee Creek Group|23354|5|Briefly described|316|||||||||
18702|Turee Creek Group|23570|5|Briefly described|p14|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
18702|Turee Creek Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
18702|Turee Creek Group|23612|5|Briefly described|p840|Archean|Archean|Of Mount Bruce Supergroup.||||||07-NOV-08
18702|Turee Creek Group|23774|6|Mentioned|p733 table 1|||Of Mount Bruce Supergroup.||||||
18702|Turee Creek Group|23870|6|Mentioned|p224 Fig. 1|||Of Mount Bruce Supergroup.||||||
18702|Turee Creek Group|23890|4|Described|p16|Paleoproterozoic|Archean|Geological Province: Pilbara Craton.  Maximum thickness: >3000m.||||||07-NOV-08
18702|Turee Creek Group|24025|5|Briefly described|p14|Paleoproterozoic|Archean|Of Mount Bruce Supergroup.  Geological Province: Hamersley Basin.||||||07-NOV-08
18702|Turee Creek Group|24169|5|Briefly described|p666 Fig. 5|||||||||
18702|Turee Creek Group|24183|6|Mentioned|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
18702|Turee Creek Group|24203|5|Briefly described|p292 Fig. 7|||Age: 2600-2500 Ma.||||||16-JAN-07
18702|Turee Creek Group|24231|6|Mentioned|p186 Fig.2|||Geological Province: Hamersley Basin.||||||
18702|Turee Creek Group|24391|6|Mentioned|p8-2 Fig.1|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
18702|Turee Creek Group|24544|4|Described|p6, 54|Paleoproterozoic|Paleoproterozoic|Of Mount Bruce Supergroup. Conformably overlies Hamersley Group. Unconformably overlain by Lower Wyloo Group. Turbidites, shallow marine carbonates, and fluvial to marine siliclastic rocks. Geological Province: Hamersley Basin.||||||07-NOV-08
18702|Turee Creek Group|24602|5|Briefly described|p854 Fig. 1|Paleoproterozoic|Archean|Age: 3.0 - 2.4 Ga.||||||07-NOV-08
18702|Turee Creek Group|24607|5|Briefly described|p968 Fig. 1, 969|||Includes Kazput, Koolbye and Kungarra Formations.||||||30-NOV-10
18702|Turee Creek Group|35976|2|Defined|p110|Proterozoic|Proterozoic|||||||
18702|Turee Creek Group|36642|6|Mentioned|Table 1|||||||||
18702|Turee Creek Group|36902|6|Mentioned|p15|||||||||
18702|Turee Creek Group|37299|6|Mentioned|Fig.1|||||||||
18702|Turee Creek Group|37327|4|Described|p395|||||||||
18702|Turee Creek Group|37460|3|Fully described|p119|||||||||
18702|Turee Creek Group|37934|6|Mentioned|Fig.1|||||||||
18702|Turee Creek Group|38321|6|Mentioned|Table 1|||||||||
18702|Turee Creek Group|38482|6|Mentioned|p15|||||||||
18702|Turee Creek Group|38790|6|Mentioned|p162|||||||||
18702|Turee Creek Group|39200|6|Mentioned|p294|||||||||
18702|Turee Creek Group|40103|6|Mentioned|p197|||||||||
18702|Turee Creek Group|40105|6|Mentioned|Fig.3|||||||||
18702|Turee Creek Group|40369|6|Mentioned|p3|||See also Plate 1||||||
18702|Turee Creek Group|40839|6|Mentioned|Fig.1|||||||||
18702|Turee Creek Group|40905|6|Mentioned|p70|||||||||
18702|Turee Creek Group|40937|6|Mentioned|p27|||||||||
18702|Turee Creek Group|40938|6|Mentioned|p8|||||||||
18702|Turee Creek Group|41349|6|Mentioned|p4|||||||||
18702|Turee Creek Group|41357|6|Mentioned|p123|||||||||
18702|Turee Creek Group|41358|6|Mentioned|p144|||||||||
18702|Turee Creek Group|41768|6|Mentioned|p21|||||||||
18702|Turee Creek Group|41845|6|Mentioned|p81|||||||||
18702|Turee Creek Group|41846|6|Mentioned|p98|||||||||
18702|Turee Creek Group|41912|5|Briefly described|p20|||||||||
18702|Turee Creek Group|42013|5|Briefly described|Map Legend|Proterozoic||||||||
18702|Turee Creek Group|42020|5|Briefly described|p316|||||||||
18702|Turee Creek Group|42112|5|Briefly described|p11|||See also Fig.1||||||
18702|Turee Creek Group|42148|5|Briefly described|p685|||||||||
18702|Turee Creek Group|42190|5|Briefly described|p274|||||||||
18702|Turee Creek Group|42260|5|Briefly described|p6|||||||||
18702|Turee Creek Group|42277|5|Briefly described|p55|||||||||
18702|Turee Creek Group|42471|4|Described|p9|||||||||
18702|Turee Creek Group|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
18702|Turee Creek Group|42704|5|Briefly described|Plate 2E|Proterozoic||Lithology is mudstone, sandstone, carbonate - but no named units included in map legend.  Intruded by metadolerite sills.||||||07-AUG-08
18702|Turee Creek Group|42730|5|Briefly described|p12|||||||||
18702|Turee Creek Group|42743|5|Briefly described|map legend|Proterozoic||||||||
18702|Turee Creek Group|42744|4|Described|p5|||||||||
18702|Turee Creek Group|42785|5|Briefly described|p261, Fig.2 p263|||Of the Mount Bruce Supergroup.||||||16-JAN-07
18702|Turee Creek Group|42898|5|Briefly described|Fig.2 P341|||Of the Mount Bruce Supergroup.||||||16-JAN-07
18702|Turee Creek Group|43037|5|Briefly described|p24|||Of the Mount Bruce Supergroup.||||||16-JAN-07
18702|Turee Creek Group|43063|5|Briefly described|Fig.1,p48|||||||||
18702|Turee Creek Group|43119|5|Briefly described|p11|||||||||
18702|Turee Creek Group|43210|6|Mentioned|p1,p3,p5.||Proterozoic|||||||
18702|Turee Creek Group|43262|5|Briefly described|Map Legend||Proterozoic|||||||
18702|Turee Creek Group|43290|4|Described|p7||Proterozoic|Of the Mount Bruce Supergroup.||||||08-APR-09
18702|Turee Creek Group|43561|6|Mentioned|Fig.4,p1435|||||||||
18702|Turee Creek Group|43595|5|Briefly described|p75,fig.2-48,p218,|||Age: approx.2.4 Ga. p220||||||
18702|Turee Creek Group|44152|5|Briefly described|p163-164, p169 Fig.2-151, p179, p188-191|||Trendall (1979).||Mount Bruce Supergroup|Kungarra Formation.|Conformably overlies Hamersley Group. Is overlain unconformably by Wyloo Group.|Mainly fine-grained greywacke, sandstone and siltstone; local carbonate and quartzite.|
18702|Turee Creek Group|44867|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
18702|Turee Creek Group|50131|6|Mentioned|p3, p3 Fig. 1|Early Proterozoic|Archaean|Of Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||22-APR-09
18702|Turee Creek Group|50216|5|Briefly described|p208, 209|Paleoproterozoic|Paleoproterozoic|Of the Mount Bruce Supergroup. Comprises shale and metasedimentary rocks. Unconformably underlies the Wyloo Group. Geological Province: McGrath Trough, Hamersley Basin.||||||07-NOV-08
18702|Turee Creek Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
18702|Turee Creek Group|50227|5|Briefly described|p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: <2209Ma.  See also p447 Fig. 3.||||||07-FEB-11
18702|Turee Creek Group|50549|5|Briefly described|p1158|Paleoproterozoic|Archean|Of the Mount Bruce Supergroup.||||||07-NOV-08
18702|Turee Creek Group|60373|4|Described|p145 Tb. 1|Paleoproterozoic|Archean|Of Mount Bruce Supersequence. Includes Kazput, Koolbye and Kungarra Formations. Geological Province: Hamersley Province.||||||
18702|Turee Creek Group|60539|5|Briefly described|p498 Fig.1|Paleoproterozoic|Archean|Geological Province: Pilbara Craton. Of the Mount Bruce Supergroup.||||||07-NOV-08
18702|Turee Creek Group|60706|5|Briefly described|p622|||Top unit of the Mount Bruce Supergroup. Conformably overlies Hamersley Group. Geological Province: Hamersley Basin.||||||
18702|Turee Creek Group|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
18702|Turee Creek Group|61268|5|Briefly described|p78 Fig.1|||Of the Mount Bruce Supergroup.||||||
18702|Turee Creek Group|61276|5|Briefly described|p578, 577|Siderian|Siderian|Orthoquartzites in Turee Creek syncline previously interpreted as Beasley River Quartzite (Wyloo Group). These rocks intruded by mafic sill with SHRIMP Pb/Pb baddelyite age of 2208 +/-10 Ma. This interpretation implies no Lower Wyloo Group in Turee Creek syncline. Age Turee Creek retroarc approx. 2450-2405 Ma.||||||17-OCT-16
18702|Turee Creek Group|61526|5|Briefly described|p879, p882|Proterozoic|Proterozoic|Sedimentary wedge thinning to the north. In the south comprises dominantly turbidites which contain diamictite, with shallower facies at the top (stromatolitic carbonates and sandstones with some conglomerates. Age: ca 2450Ma at base.||||||27-JAN-06
18702|Turee Creek Group|62129|3|Fully described|p5, p11, p13 Fig. 1, p19, p23 Fig. 3|Proterozoic||Of Mount Bruce Supergroup. Includes Kungarra, Koolbye and Kazput Formations. Conformably overlies Boolgeeda Iron Formation, overlian unconformably by Wyloo Group. Thickness: 4000m. Geological Province: Hamersley Basin.||||||07-FEB-11
18702|Turee Creek Group|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Bruce Supergroup. Includes Kungarra, Koolbye and Kazput Formations. Geological Province: Hamersley Basin, Pilbara Craton.||||||23-MAR-09
18702|Turee Creek Group|62579|5|Briefly described|p116|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Pilbara Craton. Dominantly clastic sedimentary rocks.||||||07-NOV-08
18702|Turee Creek Group|63153|5|Briefly described|p1359, p1362 Fig.3.|||||Of the Mount Bruce Supergroup.||Conformably overlies the Hamersley Group. Is overlain unconformably by Wyloo Group.|Shallow-water terrigenous clastic and chemical sedimentation.|
18702|Turee Creek Group|63367|5|Briefly described|p230, |||||Of the Mount Bruce Supergroup.||Overlies the Hamersley Group.||
18702|Turee Creek Group|63866|5|Briefly described|p151, p154|||||Mount Bruce Supergroup||Conformably (transitionally) overlies the Hamersley Group. Unconformably overlies the Wyloo Group.|Turbidites, carbonates and fluvial/marine siliciclastic rocks.|
18702|Turee Creek Group|63869|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|||Unit in Mount Bruce Supergroup.||||
18702|Turee Creek Group|64326|5|Briefly described|p70|Archean|Archean|Basal part of Mount Bruce Supergroup. Geological province: Hamersley Basin.||||||07-FEB-11
18702|Turee Creek Group|64384|4|Described|p29 Tb. 5, p37, p40|Paleoproterozoic||Of Mount Bruce Supergroup. Conformably overlies Hamersley Group. Age: ~2300Ma (p82). Geological province: Hamersley Basin.||||||07-FEB-11
18702|Turee Creek Group|64573|6|Mentioned|p784|||Geological Province: Pilbara Craton. Clastic sedimentary rocks.||||||07-FEB-11
18702|Turee Creek Group|64580|4|Described|map legend||Paleoproterozoic|Of Mount Bruce Supergroup. Mudstone; siltstone; sandstone; conglomerate; local stromatolitic dolomite; and basalt; metamorphosed.||||||09-DEC-08
18702|Turee Creek Group|64722|5|Briefly described|Fig. 2 p3-6, p7, 23|Rhyacian|Siderian|Foreland basin sequence.||||Conformably overlies the Hamersley Group. Unconformably overlain by Wyloo Group.||11-APR-12
18702|Turee Creek Group|64724|4|Described|p43, p42 Fig. 3|Siderian|Siderian|Deposited in a foreland basin setting during the Hamersley Compression event, which occurred from 2450-2405 Ma. Intruded by mafic sills 2208 +/- 10 Ma.||||||02-APR-12
18702|Turee Creek Group|64728|6|Mentioned|p94 Fig.1, p107.|||Intruded by c.2208 Ma dolerite sills.||||Overlies Woongara Rhyolite of Hamersley Group.||
18702|Turee Creek Group|65194|5|Briefly described|p98 Fig.4.23|||Unit in Mount Bruce Supergroup.||||||
18702|Turee Creek Group|65506|6|Mentioned|p987 Fig.1A|||||||||
18702|Turee Creek Group|65683|5|Briefly described|p799, p801 Fig2|||Of Mount Bruce Supergroup. Overlies Boolgeeda Iron Formation.||||||08-MAR-12
18702|Turee Creek Group|65830|6|Mentioned|p3|||||Of the Mount Bruce Supergroup.||||
18702|Turee Creek Group|66217|5|Briefly described|p44.|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.|c.2300 Ma (Trendall et al. 2004).|||||
18702|Turee Creek Group|66359|5|Briefly described|e96|||Said to be intruded by dolerite sills of 2208 +/-10 Ma  (Muller at al 2005). Intruded by undated discordant dolerites probably younger than the 2208 Ma dolerites.||||||
18702|Turee Creek Group|66574|5|Briefly described|p912-913, p916-919 Figs.4,6,8|||Mount Bruce Supergroup. Overlies the Hamersley Group. Is intruded by dolerite sills and dykes.||||||
18702|Turee Creek Group|66887|6|Mentioned|p2, p20-21|||Pilbara Craton.||||||15-DEC-16
18702|Turee Creek Group|66950|6|Mentioned|p12|||||||Overlain by the Wyloo Group.||
18702|Turee Creek Group|67025|4|Described|pp318-320.|Paleoproterozoic|Paleoproterozoic|Hamersley Basin, Pilbara Block. Over 5 km thick.||Unit in Mount Bruce Supergroup.||Conformably overlies Hamersley Group. Is overlain unconformably by the Wyloo Group.|Fine- to coarse-grained siliciclastic rocks with local occurrences of chemical sediments.|
18702|Turee Creek Group|67056|5|Briefly described|p419 Fig.2, p422, p423. |Paleoproterozoic|Paleoproterozoic|Clastics, about 5 km thick.|c.2.45 - 2.30 Ga.|Unit in Mount Bruce Supergroup.||Conformably overlies Hamersley Group.||
18702|Turee Creek Group|67130|5|Briefly described|p1, p5, p6, p24 fig 17|Rhyacian|Siderian|Deformed at 1.78 Ga. Deposited as part of a clastic wedge during orogenesis. See also p31, p33 fig 27, p34, p36, p41 fig 39.|2450 Ma - 2210 Ma|Mount Bruce Supergroup|Includes Kungarra Formation, Koolbye Formation, Kazput Formation|Conformably overlies Hamersley Group, unconformably overlain by Wyloo Group, Lower, Beasley River Quartzite|Greyish-green siltstone, fine grained wacke, fine grained sandstone, mudstone, thin to thick carbonates and glacial conglomerates and diamictites.|
18702|Turee Creek Group|67183|5|Briefly described|p640, p642, p644, p645 Tb.1|Paleoproterozoic|Neoarchean|Absent in the Oakover Basin, present in the Southern Pilbara. Misspelt as Turee Group on p644.||Mount Bruce Supergroup|Kazput Formation, Koolbye Formation, Kungarra Formation|Overlies Fortescue and Hamersley Groups.||
18702|Turee Creek Group|67201|4|Described|p32, p33 Fig.17, p34 Fig.18 see comments|||McGrath Trough. Woogarra Rhyolite is common source. Page location continued: p35, p53 Fig.40.|between c. 2450 and c. 2210 Ma||Kungarra Formation|Apparently conformably overlies Hamersley Group.|Shale and clastic metasedimentary rocks, which include glacigene rocks.|
18702|Turee Creek Group|67229|6|Mentioned|p3|||Pilbara region.||Mount Bruce Supergroup.||||
18702|Turee Creek Group|67721|6|Mentioned|p38 Fig.9||||||||Comprises siltstones, awckes, sandstones, quartzites, carbonates, and shales.|
18702|Turee Creek Group|67843|6|Mentioned|p33.|||Hamersley Basin.||||||
18702|Turee Creek Group|67855|5|Briefly described|p211, 212, 223, 224, 231|||Hamersley Basin.||Of Mount Bruce Supergroup.||Unconformably overlain by Wyloo Group.||
18702|Turee Creek Group|68035|4|Described|p292, 283, 284 Fig 1, 292 Fig 6|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.  Prior to 2007 included in Pilbara Craton, but now considered to overlie it.|||Includes Kungarra Formation, Koolbye Formation, Kazput Formation.|Conformably overlies Hamersley Group. Unconformably overlain by Wyloo Group.|Consists largely of greyish-green siltstone, fine-grained greywacke, and fine grained sandstone, but also contains thin-thick carbonate units and glacially-deposited conglomerates, diamictites and quartzite.|
18702|Turee Creek Group|68056|6|Mentioned|p170|Proterozoic|Proterozoic|||||||
18702|Turee Creek Group|68280|5|Briefly described|p1, p5, p44, p53, p54-p62|Paleoproterozoic|Paleoproterozoic||c. 2400 Ma||Includes Kazput Formation, Koolbye Formation, Kungarra Formation|Overlain by Wyloo Group, unconformably overlain by Beasley River Quartzite|Fine to medium grained sandstone and mudstone with interbedded thin carbonate rocks.|18-JAN-23
18702|Turee Creek Group|68981|6|Mentioned|p21|Paleoproterozoic|Archean|Pilbara Craton. Overlies Archean granite-greenstone terranes. Volcanic and sedimentary rocks.||||||
18702|Turee Creek Group|69003|5|Briefly described|p4, p7-9|||Capricorn Orogen. Retro-foreland basin deposits from the eroded Ophthalmia Fold Belt. Up to 4km thick.|||Kungarra, Koolbye, Kazput Formations.|||
18702|Turee Creek Group|69028|5|Briefly described|Map Legend|Rhyacian|Siderian|Turee Creek Basin. These three Formations are mapped as a single unit.|2445-2210 Ma.||Includes Kungarra, Koolbye and Kazput Formations.||Includes mudstone, siltstone, sandstone, conglomerate, local stromatolitic dolomite, and basalt; metamorphosed.|18-SEP-15
18702|Turee Creek Group|69080|4|Described|p684, p687-688, p698|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin, Pilbara Craton. Deposition occurred during early foreland-basin stage of the 2215-2145 Ma Ophthalmian Orogeny. Maximum thickness 4 km.|<c.2445 Ma.|||Unconformably overlain by Wyloo Group.|Sandstone, siltstone, dolostone and diamictite.|
18702|Turee Creek Group|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Mount Bruce Supergroup|||Undivided; mudstone; siltstone; sandstone; conglomerate; local stromatolitic dolomite; and basalt; metamorphosed.|
18702|Turee Creek Group|69185|4|Described|GEOL_LUT_CSV files||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 Mount Bruce Supergroup.|||Undivided; mudstone; siltstone; sandstone; conglomerate; local stromatolitic dolomite; and basalt; metamorphosed|
18702|Turee Creek Group|69387|6|Mentioned|p6|||||||||
18702|Turee Creek Group|69538|5|Briefly described|p516-517 Figs.2-3, p520, p559 Fig.34|Paleoproterozoic|Paleoproterozoic||2.40 Ga.|Unit in Mount Bruce Supergroup.||Overlies Hamersley Group. Is overlain by Wyloo Group.||
18702|Turee Creek Group|69543|6|Mentioned|p86-87, 92, 94||||2.4 Ga.||Meteorite Bore Member.|||
18702|Turee Creek Group|69565|5|Briefly described|p131-132, p133 Fig.1, p140|||Hamersley Province. Sediments deposited during the Great Oxidation Event.|c.2420 Ma.|Mount Bruce Supergroup.|Kungarra, Koolbye, Kazput Formations.|Conformably overlies Boolgeeda Iron Formation (topmost Hamersley Group). Is overlain by Wyloo Group.||
18702|Turee Creek Group|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||||||
18702|Turee Creek Group|69596|5|Briefly described|p1-2, p4-5, p7, p8 Fig.5|||Ophthalmia Fold Belt, Capricorn Orogen. ~4km thick.|>c.2445 Ma.||||Coarse-grained siliciclastic sedimentary rocks.|
18702|Turee Creek Group|69739|6|Mentioned|p69|||Hamersley Basin.||Mount Bruce Supergroup.||Overlies Hamersley Group.||
18702|Turee Creek Group|69745|6|Mentioned|p269-271, 273, 275-276, 281, 286-287|||Hamersley Province.||||Conformably overlies Hamersley Group. Is overlain unconformably by Lower Wyloo Group.|Basal diamictite; shales and sandstones.|
18702|Turee Creek Group|69754|5|Briefly described|p314-p319, p330, p332-p333, p339-p341|Palaeoproterozoic|Palaeoproterozoic|Pilbara Craton. A glacial diamictite has been described in  the type area. Depositional environments and changes between them are described. Outcrops in the hinges of large scale folds along the southern Hamersley Ranges.3.9 km thick. A sequence stratigraphic model from Krapez (1996) is provided.|||Includes the Kungarra Formation, Koolbye Formation and the Kazput Formation.|||
18702|Turee Creek Group|70086|5|Briefly described|p194-196,209|Rhyacian|Siderian|Geological province: Pilbara Craton. Of the Hamersley Basin. Thickness: 3-4km. Exposed in the Hamersley Range of Western Australia. Hosts carbonate and glacially-influenced strata that record onset of the Great Oxidation Event (GOE) (Bekker et al., 2004; Martin et al., 2013; Van Kranendonk and Mazumder, 2015). Records a broadly shallowing-upward profile, from deepwater Boolgeeda BIFs, to marine (Kungarra) to fluvial and shallow marine (Koolbye, Kazput) strata.|ca. 2.45-2.22 Ga|Unit of Mount Bruce Supergroup.|Includes Kazput and Kungarra formations.|Overlain unconformably by Wyloo Group. Underlain conformably by Hamersley Group.||
18702|Turee Creek Group|70327|5|Briefly described|p4, p19|||Hamersley Province. A pre-Ophthalmia Orogeny foreland basin.|||Kazput Formation.|Is overlain unconformably by Beasley River Quartzite.||15-DEC-16
18702|Turee Creek Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic||2445-2208 Ma||||Mudstone, siltstone, sandstone, conglomerate, local stromatolitic edolomite, diamictite and dolerite sills; metamorphosed.|
18702|Turee Creek Group|70814|5|Briefly described|p34-p35|Paleoproterozoic|Paleoproterozoic||2445-2208 Ma|||||
18702|Turee Creek Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||||Conformably overlies the Hamersley Group, upper. Unconformably overlain by the Shingle Creek Group.||
18702|Turee Creek Group|70936|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province, Pilbara Craton.||||||
18702|Turee Creek Group|70949|5|Briefly described|p988-989|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin. Deposited during the 2215-2145 Ma Ophthalmian Orogeny.||||||
18702|Turee Creek Group|70958|4|Described|p2-4, Fig. 1|Paleoproterozoic|Paleoproterozoic|||Of Mount Bruce Supergroup|Includes Kungarra Formation and unnamed overlying unit.||Upper part: basal conglomerate overlain by impure clastics, sandstone with rare pebbles to shale. Overlain by carbonates.|
18702|Turee Creek Group|71003|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||||||
18702|Turee Creek Group|71042|5|Briefly described|p65-p67, p72, p75, p98|||[Referred to as the Turee Group on p67 and the author mistakenly attempts to assign this group to the Hamersley Group p65 and following pages].|||Includes the Kungarra Formation, Koolbye Formation, Kazput Formation.|||24-MAY-19
18702|Turee Creek Group|71112|4|Described|p68-72,75,78-80,83|||Geological province: Pilbara Craton. Of the Turee Creek Basin (compressive basin). Intruded by two massive, coarse-grained dolerite sills post-dating Woongarra Volcanics (containing 2208+\-10 Ma baddeleyite; SHRIMP U-Pb; Muller et al., 2005), which are folded concordantly with the Turee Creek Group and truncated by basal unconformity with the Beasley River Quartzite. Youngest detrital-zircon provenance for combined samples are 2440+\-16 Ma, overlapping with 2449+\-3 Ma age of Woongarra Volcanics (Barley et al., 1997).||Unit of Mount Bruce Supergroup.||Overlain unconformably by Beasley River Quartzite.||
18702|Turee Creek Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||turbidite|
18702|Turee Creek Group|71513|6|Mentioned|p66 fig 1,|||Pilbara Craton.||||||
18702|Turee Creek Group|71550|4|Described|p34-36,38,44-47|Rhyacian|Paleoproterozoic|Geological province: Of Hamersley Basin. Abbreviated as TCG in text. Thickness: c. 4000m. Metamorphosed up to sub-greenschist facies. Records a near continuous sedimentary sequence deposited during the rise of atmospheric oxygen and comprises at least two glacial diamictite horizons. Sedimentation occurred in an asymmetric basin, called the McGrath Trough, which reflects flexural subsidence driven by the migration to the NE of a geanticline or a thrust-fold belt system (Horwitz, 1982; Blake and Barley, 1992; Martin, 1999; Martin et al., 2000). Intruded by a dolerite sill dated, folded and truncated by Beasley River Quartzite, dated at 2208+\-10 Ma (Muller et al., 2005). Krapez et al. (2017) presented maximum ages of ca. 2.44 Ga. Deposition likely occurred in a minimum timespan of 100my, bracketed between the 2.31 Ga Re-Os age of the MBM glaciation and the 2208+\-10 Ma dolerite sill intruding the TCG (M¿ller et al., 2005). Detrital provenance is likely from erosive products of underlyng Hamersley Province and Pilbara basement.|||Includes Kazput, Koolbye and Kungarra formations.|Overlain unconformably by lower Wyloo Group/Beasley River Quarzite. Underlain by Boolgeeda Iron Formation (Hamersley Group).||03-SEP-19
18702|Turee Creek Group|71803|5|Briefly described|p366-p368|||||Mount Bruce Supergroup||||
18702|Turee Creek Group|71808|4|Described|v, viii, ix, xi, p5-p6, p10|||Hamersley Province. Interpreted to be a foreland basin unit. See also p42, p74, p117, p156, p164.|c. 2450 Ma|Mount Bruce Supergroup|Includes the Three Corner Bore Member.|Conformably overlies the Boolgeeda Iron Formation (Hamersley Group). Overlain by the Lower Wyloo Group.||
18702|Turee Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Mount Bruce Supergroup|Includes Kazput Formation, Koolbye Formation, Kungarra Formation, Boolgeeda Iron Formation|Intruded by Balgara Dolerite sills.|Mudstone, siltstone, sandstone, conglomerate, dolomite; minor diamictite, limestone and iron formation; intruded by Balgara Dolerite sills.|
18702|Turee Creek Group|72254|6|Mentioned|App.A p11|||||||Underlain by Hamersley Group. Unconformably overlain by Wyloo Group.||
18702|Turee Creek Group|72493|5|Briefly described|p28, 30|||Hamersley Basin.|2.44 - 2.21 Ga.|Topmost Mount Bruce Supergroup.||Overlies Hamersley Group.||
18702|Turee Creek Group|72569|6|Mentioned|p2|||Of the Hamersley Basin.||Mount Bruce Supergroup||Overlies the Hamersley Group.||
18702|Turee Creek Group|72570|5|Briefly described|p1-8, p12-16|Orosirian|Siderian|Features diverse stromatolite and macrofossil morphology in addition to the appearance of clotted (thrombolite-like) microbialites. Microbialite morphology and biodiversity is discussed in detail. C. 4000m thick.|c. 2000-2400 Ma|Mount Bruce Supergroup|Includes Kungarra Formation, Koolbye Formation and the Kazput Formation.|||
18702|Turee Creek Group|72712|4|Described|p1, p2, p3, p5-6, p4 Fig.2, p9, p14-25.|Rhyacian|Siderian|See also p30, p42, p44, p49, p50, p53, p55-56, p63. Part of the Turee Creek Basin (Formerly McGrath Trough). Shown on p63 (back cover summary). Folding of this group is constrained to >2008 Ma by undeformed Panhandle Dolerite. Approximateyl 4km thick formerly considered a Formation within the Wyloo Grup of Macleod et al (1963). Conformably overlies the Boolgeeda Iron Formation.|c. 2310 Ma to 2208 +/- Ma.|Mount Bruce Supergroup|Anthiby Formation, Munder Formation, Kazput Formation, Koolbye Formation, Kungarra Formation, Meteorite Bore Member.|Shown to be gradationally to disconformably overlying Hamersley Group and underlying Wyloo Group. Intruded by Balgara Dolerite.|Includes conglomerate, shale and find sandstone, dolerite, dolomite with limestone and marl.|14-JAN-21
18702|Turee Creek Group|72758|5|Briefly described|p4 Fig.1, p6, p14 Tb.1, p23, p27-29.|Archaean|Archaean|Represents shallowing marine to fluvial succession. Maximum thickness almost 4 km in Hardey Syncline.  Thins rapidly to zero to NW.  Previously (before 1979) Turee Creek Formation.||Mount Bruce Supergroup|Includes Kungarra Formation.|Conformably overlies Boolgeeda Iron Formation, Hamersley Group and unconformably underlies Wyloo Group. Intruded by dolerite sills.|Includes conglomerate, lithic ard quartzitic arenites, wacke, mudstone, pebble-cobble mudstone, dolomite, basalt; intruded by dolerite sills.|
18702|Turee Creek Group|73022|6|Mentioned|p2, p3 Fig.2|||||Mount Bruce Supergroup||Overlies the Hamersley Group|Includes siliciclastic sedimentary rocks.|
18702|Turee Creek Group|73102|6|Mentioned|p2 Fig.1|||||||||
18702|Turee Creek Group|73290|6|Mentioned|p784|||Hamersley Province.||||||
18702|Turee Creek Group|73442|6|Mentioned|p2 Fig.1|||||||||
18702|Turee Creek Group|73538|4|Described|p1-8, App TbS1|Rhyacian|Siderian|Hamersley Basin. Deposited during the Great Oxidation Event and at least two other glacial episodes. Approximately 4 km thick. Uppermost unit of the Mount Bruce Supergroup. Records a marked shift in Nd isotope compositions. Interpreted as being mainly derived from the underlying Hamersley and Fortescue groups.|2.45 to 2.2 Ga|Mount Bruce Supergroup|Kazput Formation, Koolbye Formation, Kungarra Formation|Conformably underlain by Boolgeeda Iron Formation, Hamersley Group. Unconformably overlain by Beasley River Quartzite, Wyloo Group.|Siliciclastic sediments including mudstone/siltstones and glacial diamictites.|
18702|Turee Creek Group|75075|6|Mentioned|p420 Fig.1, 424|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||Mount Bruce Supergroup.||||
18707|Turkey Hill Formation|22716|6|Mentioned|table4,p231|Neoproterozoic III|Neoproterozoic III|Age: 610Ma||||||
18707|Turkey Hill Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin.||||||30-SEP-08
18707|Turkey Hill Formation|22901|6|Mentioned|74|||Geol province Officer Basin.||||||30-SEP-08
18707|Turkey Hill Formation|41751|6|Mentioned|p8|||||||||
18707|Turkey Hill Formation|61732|3|Fully described|p58 Fig. 22, p86|Cryogenian|Cryogenian|Comprises sandstone, siltstone, claystone and diamictite; probably a marine glacial tillite. Several hundred metres thick. Overlain by Paterson Formation. Geological Province: southern Officer Basin.||||||18-JUL-13
18707|Turkey Hill Formation|62453|3|Fully described|p5 Fig. 3, 47|Ediacaran|Ediacaran|Geological Province: Officer Basin. Sandstone, siltstone, mudstone, diamictite. Unconformably overlain by Paterson Formation.||||||
18707|Turkey Hill Formation|62987|6|Mentioned|p30|||In the Paterson Orogen.||||||
18707|Turkey Hill Formation|64580|4|Described|map legend||Neoproterozoic|Sandstone, siltstone and mudstone; possibly diamictite.||||||09-DEC-08
18707|Turkey Hill Formation|64970|5|Briefly described|p718, p719 Fig. 2|Neoproterozoic|Neoproterozoic|Tillites and fluvio-glacial deposits. Geological Province: Officer Basin.||||||27-MAY-09
18707|Turkey Hill Formation|65102|4|Described|p366,368, 371 Figs.4-41,4-45, Table4-15|Neoproterozoic|Neoproterozoic|Officer Basin. Several hundred metres; sandstone, siltstone, claystone; minor tillite; shallow water glacial; unconformable on granite basement; type section at Miller Soak, 28deg 07min S, 124deg 16min E; unfossiliferous; Sturtian or Marinoan from stratigraphic correlation.||||||
18707|Turkey Hill Formation|65410|5|Briefly described|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin.|||||Tillite.|
18707|Turkey Hill Formation|65416|5|Briefly described|p137, p141.|Neoproterozoic|Neoproterozoic|Officer Basin; exposed on the western margin. Could be included in Supersequence LP2 or LP3.|||||Sandstone, siltstone, claystone and minor diamictite.|
18707|Turkey Hill Formation|68270|4|Described|p678,682-684,687|Cryogenian|Cryogenian|Western Officer Basin. Type section occurs in Miller Soak; lat, 28'9.4"S, long, 124'16.5"E. Exposed in the southwestern part of the western Officer Basin and is several hundreds of metres thick. ?Glacial in part (glacial component may be Phanerozoic). Related to Elatina glaciation.||||Overlain unconformably by Patterson Formation.|Sandstone, mudstone, diamictite (diamictite may be from overlying Patterson Formation).|03-JUL-19
18707|Turkey Hill Formation|68277|6|Mentioned|p96, 103|Neoproterozoic|Neoproterozoic|||||||
18707|Turkey Hill Formation|69152|5|Briefly described|500k_geologyp08_lut||Neoproterozoic||||||Sandstone, siltstone and mudstone; possibly diamictite.|07-AUG-15
18707|Turkey Hill Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Cryogenian|Officer Basin (Phase 1). 500k_interpgeop14_lut.csv.|850 - 541 Ma (inferred).||||Sandstone, siltstone and mudstone; possibly diamictite,|
18707|Turkey Hill Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Cryogenian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny; Paterson Orogeny; Petermann Orogeny.|850-541 Ma (inferred)||||Sandstone, siltstone and mudstone; possibly diamictite|
18707|Turkey Hill Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
18707|Turkey Hill Formation|71270|4|Described|GEOL_LUT_CSV files|Ediacaran|Cryogenian|Of Officer Basin, 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_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|720-541 Ma (inferred)||||Sandstone, siltstone and mudstone; possibly diamictite|
18707|Turkey Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Cryogenian|Officer Basin (Phase 1).|||||Sandstone, siltstone and mudstone; possibly diamictite.|
18710|Turner Granite|30766|6|Mentioned|p19|||||||||
18718|Turnstone Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Late Cretaceous|Late Creatceous|Mory (1988). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Calcareous claystones and calciluties.  Also on p228 Fig. 18.||||||01-MAR-10
18718|Turnstone Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Maastrichtian|Campanian|150-200m thick, open marine shelf deposits, fossiliferous. Only in east Ashmore Platform. Type section: Turnstone 1 well (925-1120m).||Bathurst Island Group||Overlies Vee Formation (conformably but diachronous). Grades laterally into Puffin Formation. Equivalent to upper Wangarlu Formation.|Calcareous claystone; minor marl.|
18718|Turnstone Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
18718|Turnstone Formation|41532|2|Defined|p308|Late Cretaceous||||||||
18718|Turnstone Formation|42442|2|Defined|p29|Maastrichtian|Campanian|Variation of Turnstone formation, WA. Age Late Cretaceous (Campanian to Maastrichtian).||||||01-SEP-14
18718|Turnstone Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
18718|Turnstone Formation|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
18718|Turnstone Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
18718|Turnstone Formation|60385|5|Briefly described|p270, p272 Fig 3|Maastrichtian|Campanian|Browse Basin.|||Includes Prudhoe Member, Puffin Member, Puffin Sandstone Member, Borde Marl Member||Mudstone, with sandstone and hemipelagic marl members.|
18718|Turnstone Formation|61548|6|Mentioned|p480 Fig.3|Maastrichtian|Campanian|Northern Bonaparte Basin.||||||
18718|Turnstone Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Age: ~77-~65Ma. Geological Province: Northern Bonaparte Basin.||||||01-MAR-10
18718|Turnstone Formation|64695|5|Briefly described|p262 Fig.8 |Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Overlies Fenelon Formation. Is overlain by Johnson Formation.||
18718|Turnstone Formation|68223|6|Mentioned|p178 Fig.3|Maastrichtian|Campanian|||||||
18718|Turnstone Formation|69452|6|Mentioned|p36:15|||Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
18718|Turnstone Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Maastrichtian|Campanian|See also Sahul: Fig.2, p2. Vulcan: Fig.2.||Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||12-JUL-16
18745|Two Gum Monzogranite|42705|5|Briefly described|map legend|Archean||Reserved as Two Gum Granite.||||||07-NOV-08
18745|Two Gum Monzogranite|42988|5|Briefly described|Map Legend|||||||||
18745|Two Gum Monzogranite|42989|3|Fully described|p21|||||||||
18745|Two Gum Monzogranite|43101|3|Fully described|p48|||||||||
18745|Two Gum Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
18745|Two Gum Monzogranite|60076|5|Briefly described|p46 App. 1|||[Agmtg]   Medium-grained, porphyritic, biotite-hornblende monzogranite.||||||
18745|Two Gum Monzogranite|65204|6|Mentioned|p18 Tbl.3.|Neoarchean||0.5-7mm grains; porphyritic||||||
18745|Two Gum Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Medium-grained, porphyritic, biotite-hornblende monzogranite.||||||07-FEB-11
18745|Two Gum Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained, porphyritic, biotite-hornblende monzogranite.|07-AUG-15
18745|Two Gum Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained, porphyritic, biotite-hornblende monzogranite|
18745|Two Gum Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
18745|Two Gum 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)||||Medium-grained, porphyritic, biotite--hornblende monzogranite|
18752|Tyler Formation|41997|6|Mentioned|p72|||||||||
18795|Ullawarra Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Overlying unit Coodardoo Formation, underlying unit Devil Creek Formation.  Max. thickness:  650m.  See also p54.||||||24-JAN-06
18795|Ullawarra Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
18795|Ullawarra Formation|23485|4|Described|p31|Paleoproterozoic|Paleoproterozoic|Of Edmund Group.||||||07-NOV-08
18795|Ullawarra Formation|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
18795|Ullawarra Formation|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Curran Formation. U'lying unit Devil Creek Formation. Geological Province: Bangemall Basin. Max. thickness: 650 m.||||||
18795|Ullawarra Formation|24115|4|Described|p3, p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 650m. Overlies the Devil Creek Formation. Overlain by the Coodardoo Formation. Geological Province: Edmund Basin.||||||
18795|Ullawarra Formation|24183|2|Defined|p4 Fig.3, p17|Calymmian|Statherian|Of the Edmund Group (Martin et al. 1999a). Overlain by Coodardoo Formation. Max. Thickness: 650m. Conformably overlying the Devil Creek Formation. Minimum age constrained by dolerite sill (1449 +/-5 Ma). Maximum age same as Edmund Group: ~1620 Ma.||||||21-MAR-11
18795|Ullawarra Formation|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Devil Creek Formation. Overlain by Coodardoo Formation.||||||
18795|Ullawarra Formation|29845|6|Mentioned|Table 68|||||||||
18795|Ullawarra Formation|29916|4|Described|p118|||||||||
18795|Ullawarra Formation|30881|4|Described|p525|||||||||
18795|Ullawarra Formation|34124|5|Briefly described|Table 1|||Upper Proterozoic. See also PP9,10,11,14||||||
18795|Ullawarra Formation|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18795|Ullawarra Formation|35982|6|Mentioned|Table 22|||||||||
18795|Ullawarra Formation|36551|6|Mentioned|p101|||||||||
18795|Ullawarra Formation|36884|4|Described|p154|||||||||
18795|Ullawarra Formation|37460|4|Described|Table 3.VI|||||||||
18795|Ullawarra Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
18795|Ullawarra Formation|38299|5|Briefly described|p10|||||||||
18795|Ullawarra Formation|39171|6|Mentioned|p82|||||||||
18795|Ullawarra Formation|39210|5|Briefly described|Table 2|||||||||
18795|Ullawarra Formation|39370|5|Briefly described|p32|||||||||
18795|Ullawarra Formation|40088|6|Mentioned|p227|||||||||
18795|Ullawarra Formation|40089|2|Defined|p31|Mesoproterozoic|Mesoproterozoic|||||||
18795|Ullawarra Formation|40899|6|Mentioned|Fig.1|||||||||
18795|Ullawarra Formation|41360|6|Mentioned|p192|||||||||
18795|Ullawarra Formation|42471|4|Described|p21|||Probably equivalent to Fords Creek Shale.||||||
18795|Ullawarra Formation|42472|5|Briefly described|Map legend|||||||||
18795|Ullawarra Formation|44142|4|Described|p313 Tb.4-4, p318-319, p321, p327 Tb.4-5|||1500-2500m thick. Shallow marine platform deposits, sand and silt shoals, turbidity currents. Within Dooley Subgroup of Chuck (1984). Contrasting paleoenvironmental interpretations.||Edmund Subgroup.||Overlies Devil Creek Formation, Nanular Sandstone or Discovery Chert conformably, and Mount James Formation unconformably. Overlain by Curran Formation conformably.|Shale, siltstone, fine-grained arenite; minor interbeds of wacke, claystone, dolomite, chert. Contains numerous dolerite sills.|13-MAR-18
18795|Ullawarra Formation|44319|14|Not recorded|map legend||Mesoproterozoic|Bangemall Group. M.Proterozoic.||||||
18795|Ullawarra Formation|50225|4|Described|p387 Fig. 2, p395|||Of Edmund Gp. Planar + ripple-laminated siltstone + mudstone, with minor dolostone + fine- to medium-grained sandstone. Uppermost unit is Curran Mbr. Conformably overlies Devil Creek Fm. Max. thick: 2000m. Contains former Nanular Sst?||||||07-FEB-11
18795|Ullawarra Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup).||||||07-NOV-08
18795|Ullawarra Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin.||||||07-NOV-08
18795|Ullawarra Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
18795|Ullawarra Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Underlies the Curran Member. Siltstone, sandstone, dolostone and minor chert.||||||07-NOV-08
18795|Ullawarra Formation|63470|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Siltstone, fine-grained sandstone, dolostone and chert; intruded by numerous dolerite sills.||||||24-SEP-07
18795|Ullawarra Formation|63471|5|Briefly described|Map legend|Mesoproterozoic||Of the Edmund Group (Bangemall Supergroup). Underlies the Curran Member of the Coodardoo Formation. Geological Province: Edmund Basin. Siltstone, fine-grained sandstone; dolostone and minor chert; intruded by numerous dolerite sills.||||||24-SEP-07
18795|Ullawarra Formation|63866|5|Briefly described|p162|||||Edmund Group||||
18795|Ullawarra Formation|63869|4|Described|p28, p37-39, p42, p43, p60, Plate 1|Calymmian|Statherian|Includes the former Curran Formation, downgraded to Member status (Martin et al., 1999; Martin and Thorne, 2002). 100-650 m thick (sedimentary component). Minimum age from a dolerite sill at Coodardoo Well. No known mineral deposits apart from a small manganese occurrence.|>1449 +/- 5 Ma (Wingate, 2002).|Unit in Edmund Group.|Includes Curran Member.|Conformably overlies Devil Creek Formation. Is overlain transitionally by Coodardoo Formation.|Mainly thin-bedded black and maroon siltstone and mudstone, with lesser interbedded fine- to medium-grained sandstone, and minor chert and dolostone. Characterised by large number of dolerite sills.|
18795|Ullawarra Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert, and minor conglomerate.||||||09-DEC-08
18795|Ullawarra Formation|64728|6|Mentioned|p95 Fig.2.|Mesoproterozoic|Mesoproterozoic|Deep-water siliciclastic and carbonate facies deposited below wave-base.||Unit in Edmund Group.|Includes Curran Member.|Overlies Devil Creek Formation. Is overlain by Coodardoo Formation.||
18795|Ullawarra Formation|65450|6|Mentioned|p6 Fig.4|Mesoproterozoic|Mesoproterozoic|||Edmund Group.||||06-JAN-17
18795|Ullawarra Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Over Devil Creek Formation. Age: c. 1465 Ma. Siltsone; subordinate sandstone, dolostone and chert; intruded by numerous dolerite dykes. Geol. Prov: Edmund Basin.||||||
18795|Ullawarra Formation|65506|5|Briefly described|p986, p988||1485 +/-7 Ma.|Unit in Edmund Group. Quartz-rich sandstone. U-Pb detrital zircon maximum depositional age (GSWA 148994).||||||
18795|Ullawarra Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Includes Nanular Member.  c. 1460 - <1620 Ma. Consists of siltstone; subordinate fine grained sandstone, dolostone, and chert, intruded by numerous dolerite sills (not on Map);||||||
18795|Ullawarra Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin; contains Nanular Member. Siltstone, subordinate fine-grained sandstone, dolostone, and chert, intruded by numerous dolerite sills. Overlies Devil Creek Formation.||||||06-SEP-10
18795|Ullawarra Formation|65830|4|Described|p4, p7, p10, p11, p16-17; Plates 1,2|Calymmian|Statherian|Has a large volume of intruded dolerite sills south of the Talga Fault. 100-650m thick. Deposited in a deep-marine shelf environment.||Of the Edmund Group|Includes Curran Member.|Conformably underlain by the Devil Creek Formation. Transitionally overlain by the Coodardoo Formation. Unconformably overlain by the Backdoor Formation.|Consists mainly of thin-bedded black and maroon siltstone and mudstone with lesser interbedded fine- to medium-grained sandstone, and minor chert and dolostone.|
18795|Ullawarra Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in upper Edmund Group, Bangemall Supergroup. Includes Nanular Member. Planar-laminated siltstone, locally calcareous.||||||
18795|Ullawarra Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in upper Edmund Group. Siltstone; subordinate fine-grained sandstone, dolostone, and chert; locally intruded by numerous dolerite sills. Includes 2 unnamed units; one of felsic volcaniclastic sandstone and breccia, other of sandstone and siltstone.||||||
18795|Ullawarra Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Overlies Devil Creek Formation. Age: c.1465 Ma. Siltsone; subordinate sandstone, dolostone and chert; intruded by numerous dolerite sills. Includes an unnamed unit of siltstone and thin- to thick-bedded sandstone.||||||
18795|Ullawarra Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Unit in Edmund Group. Age c.1465 Ma. Pelitic and psammitic schist; andalusite-garnet-biotite-muscovite schist.||||||
18795|Ullawarra Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Siltstone; subordinate fine-grained sandstone, dolostone and chert; locally intruded by numerous dolerite sills. Includes Nanular Member and an unnamed unit of felsic volcaniclastic sandstone and breccia.||||||
18795|Ullawarra Formation|66241|4|Described|pp1-4, p6, p9. |Calymmian|Calymmian|This age is a SHRIMP U-Pb zircon age from a volcaniclastic unit; it is within error of c.1465 Ma age of Narimbunna Dolerite.|1460 +/- 9 Ma (Wingate et al. in prep.).|Unit in Edmund Group.||Overlies Devil Creek Formation. Is overlain by Coodardoo Formation.|Mainly deep marine siltstone; minor fine-grained sandstone, dolostone and chert; includes one occurrence of highly silicified volcanic sandstone and breccia with angular to rounded lapilli.|
18795|Ullawarra Formation|66299|4|Described|pp299-304.|Mesoproterozoic|Mesoproterozoic|Contains a horizon of felsic volcanic sandstone used for dating.|1460 +/- 9 Ma.|Unit in Edmund Group.||Overlies Devil Creek Formation. Is intruded by voluminous sills of metamorphosed Narimbunna Dolerite.|Pelitic and psammitic schist; andalusite-garnet-biotite-muscovite schist.|
18795|Ullawarra Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Devil Creek Formation. Is overlain by Coodardoo Formation.|Siltstone; subordinate fine-grained sandstone, dolostone and chert; locally intruded by numerous dolerite sills.|
18795|Ullawarra Formation|67245|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|c.1460 Ma.|Unit in Edmund Group.||Overlies Devil Creek Formation.|Siltstone; subordinate fine-grained sandstone, dolostone and chert; locally intruded by numerous dolerite sills.|
18795|Ullawarra Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|c.1460 Ma.|Unit in Edmund Group.||Overlies Devil Creek Formation and, locally, Narimbunna Dolerite.|Siltstone; subordinate fine-grained sandstone, dolostone and chert; locally intruded by numerous dolerite sills.|
18795|Ullawarra Formation|67346|6|Mentioned|p796 Fig.3|Mesoproterozoic|Mesoproterozoic|||Of the Edmund Group.||||11-MAY-12
18795|Ullawarra Formation|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|c.1460 Ma.|Unit in Edmund Group.|||Siltstone; subordinate fine-grained sandstone, dolostone and chert; intruded by numerous dolerite sills.|
18795|Ullawarra Formation|68285|5|Briefly described|Map Legend|Calymmian|Calymmian|Edmund Basin. Said to be about 1460 Ma. Intruded by numerous dolerite sills.|c. 1460 Ma|Of the Edmund Group.||Underlain by the Devil Creek Formation. Overlain by Coodardoo Formation or Backdoor Formation.|Siltstone; subordinate fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills.|
18795|Ullawarra Formation|68286|5|Briefly described|Map Legend|Calymmian|Calymmian|Edmund Basin. Said to be about 1460 Ma. Intruded by numerous dolerite sills.|c. 1460 Ma|Of the Edmund Group|Informally subdivided in part into two unnamed units.|Underlain by the Devil Creek Formation. Overlain by Coodardoo Formation or Backdoor Formation.|Siltstone; subordinate fine-grained sandstone, dolostone, and chert; conglomerate; intruded by numerous dolerite sills.|
18795|Ullawarra Formation|69003|5|Briefly described|p34-35|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. The volcaniclastic components are essentially coeval with Narimbunna Dolerite intrusions.|c.1460 Ma.|Edmund Group.||Overlies Devil Creek Formation. Is overlain by Coodardoo Formation. Is intruded by Narimbunna Dolerite.|Deep-marine siltstone. Contains significant horizons of felsic volcaniclastics.|
18795|Ullawarra Formation|69010|5|Briefly described|Map Legend|Calymmian|Calymmian|Edmund Basin. Includes an unnamed and separately mapped unit of ferruginous siltstone, minor fine- to medium-grained sandstone and chert, commonly manganiferous.|c. 1460 Ma|Of the Edmund Group.|||Comprises siltstone, subordinate fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills.|24-APR-14
18795|Ullawarra Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|||Siltstone, fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills.|05-MAY-14
18795|Ullawarra Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.|Includes the Curran Member.|Underlain by the Devil Creek Formation. Overlain by the Coodardoo Formation.|Siltstone, fine-grained sandstone, dolostone, and chert; intruded by numerous dolerite sills.|05-MAY-14
18795|Ullawarra Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Devil Creek, Coodardoo and Discovery Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert and minor conglomerate.|06-MAY-14
18795|Ullawarra Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from sample (148994.1.pdf)|1461 Ma +/- 7 Ma (SHRIMP)|Edmund Group|Includes Curran Member, Nanular Member|Overlain by Curran Member, Conformably overlies Devil Creek Formation|Felsic volcaniclastic sandstone and breccia, coarse grained dolarenite, dolorudite, laminated dololutite, pelitic and psammitic schist; siltstone and thin-thickly bedded sandstone. Dolostone and chert intruded by dolerite sills; conglomerate.|
18795|Ullawarra Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 4.||Unit of Edmund Group.||||
18795|Ullawarra Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
18795|Ullawarra Formation|70019|6|Mentioned|p93|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Overlain by Coodardoo Formation. Underlain by Devil Creek Formation.||
18795|Ullawarra Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Edmund Basin. The two facies are mapped separately.|1590-1455 Ma.|Edmund Group.||Overlies Devil Creek Formation.|Siltstone, subordinate fine-grained sandstone, dolostone and chert, all intruded by numerous dolerite sills; sandstone and siltstone.|
18795|Ullawarra Formation|70136|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|<1620 - > 1460 Ma.|Edmund Group.|||Siltstone; subordinate fine-grained sandstone, dolostone and chert; intruded by numerous dolerite sills (section only).|
18795|Ullawarra Formation|70767|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|1590-1455 Ma.|Edmund Group.||Overlies Devil Creek Formation. Is overlain by Backdoor Formation.|Siltstone; subordinate fine-grained sandstone, dolostone, chert, and felsic volcaniclastic rock; intruded by numerous dolerite sills.|25-NOV-16
18795|Ullawarra Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.|1590-1455 Ma.|Edmund Group.||Overlies Devil Creek Formation. Is overlain by Backdoor Formation.|Siltstone; subordinate fine-grained sandstone, dolostone, chert, and felsic volcanic rock; intruded by numerous dolerite sills.|
18795|Ullawarra Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 143440.1.pdf, 149031.1.pdf, West Australian Craton, Edmund Basin|1590-1455 Ma|Edmund Group|Includes Curran Member|Overlain by Coodardoo Formation, Conformably overlies Devil Creek Formation, Unconformably overlain by Collier Group, intruded by Kulkatharra Dolerite|Felsic volcaniclastic sandstone, felsic metavolcaniclastic rock, breccia, coarse grained dolarenite, thick bedded dolorudite, laminated dololutite, siltstone, ferruginous siltstone; minor fine to medium grained sandstone and chert.|
18795|Ullawarra Formation|70814|4|Described|p3, p5, p13-p15||Calymmian|Edmund Basin. Together with the Discovery, Devil Creek and Coodardoo Formations forms Depositional Package 4 of the Edmund Group. Is the source for the minimum age derivation of the Edmund Group. Wingate (2010b) derived maximum depositional ages for this formation of 1463 +/- 8 Ma and 1455 +/- 9 Ma; these ages are interpreted as being close to depositional. Ranges in thickness from a mimimum of about 30m to around 1800m. Interpreted to have been deposited in a deep marine shelf environment, given the fine-grained nature of most of the rock types. Ages provided are the maximum depositional ages of this unit and includes an age of 1463 +/- 8 Ma (Wingate et al., 2010). See also p20, p22, p25-p27, p34-p35, p49, p57.|1455 +/- 9 Ma (Wingate et al., 2012a)|Edmund Group|Includes the Curran Member.|Conformably overlies the Devil Creek Formation. Conformably overlain by the Coodardoo Formation. Intruded by the Kulkatharra and Narimbunna Dolerites.|Siltstone with subordinate fine-grained sandstone, dolomite and chert.|05-MAY-23
18795|Ullawarra Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, sandstone, dolostone, claystone, shale|
18795|Ullawarra Formation|72705|5|Briefly described|p3-6, 9, 11-12|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.|c.1460 Ma (detrital zircon U-Pb).|Edmund Group.|Curran Member.|Overlies Devil Creek Formation. Is overlain by Coodardoo Formation.|Siltstone and minor sandstone.|
18795|Ullawarra Formation|73102|6|Mentioned|p22|Calymmian|Calymmian[?]|Age costraints discussed.|1590-1455 Ma|Edmund Group.||Intruded by Kulkatharra Dolerite.|Includes sandstone and siltstone.|
18795|Ullawarra Formation|73442|6|Mentioned|p18, p23|||Also referred to as part of Depositional Package 4.||||Intruded by Narimbunna Dolerite, Kulkatharra Dolerite||
19021|Utting Calcarenite|5256|5|Briefly described|p143, p148.|Visean|Visean|Bonaparte Basin. Type section is 120m thick, around Utting Gap, NW Carlton Shelf. Age: mid-Visean V2b - V3a (Holkerian). Richly fossiliferous shelf carbonates.||||||
19021|Utting Calcarenite|13194|4|Described|p389 Tb. 4-16, p402 fig 4-66|Visean|Visean|Type Section: Utting Gap 14o58'S 128o36'E. 36-64m thick marine shelf deposits.||||Overlies Milligans Formation (conformably). Overlain by Burvill Formation (conformably).|Sandy limestone, calcareous sandstone; minor sandstone.|
19021|Utting Calcarenite|23820|5|Briefly described|p202 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
19021|Utting Calcarenite|31519|6|Mentioned|p917|||||||||
19021|Utting Calcarenite|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
19021|Utting Calcarenite|32663|4|Described|Table 2|||L.Carb.||||||
19021|Utting Calcarenite|32664|6|Mentioned|Map legend|Visean|Visean|||||||
19021|Utting Calcarenite|32867|6|Mentioned|p40|||||||||
19021|Utting Calcarenite|32868|6|Mentioned|p220|||||||||
19021|Utting Calcarenite|32870|5|Briefly described|p48|||See alsop53.||||||13-DEC-06
19021|Utting Calcarenite|33621|6|Mentioned|Table 1|||||||||
19021|Utting Calcarenite|34085|6|Mentioned|Cor.chart|||Visean||||||
19021|Utting Calcarenite|34155|6|Mentioned|p93|||Lower Visean. See also pp101,102.||||||13-DEC-06
19021|Utting Calcarenite|36890|3|Fully described|p380|||||||||
19021|Utting Calcarenite|36904|6|Mentioned|p9|||||||||
19021|Utting Calcarenite|40993|6|Mentioned|Fig.1|||||||||
19021|Utting Calcarenite|41839|4|Described|p31|||Formerly "Milligans Beds".||||||23-APR-08
19021|Utting Calcarenite|41864|3|Fully described|p306|||||||||
19021|Utting Calcarenite|41865|5|Briefly described|Map legend|late Visean|early Visean|||||||
19021|Utting Calcarenite|41867|5|Briefly described|Map legend|late Visean|early Visean|||||||
19021|Utting Calcarenite|42442|6|Mentioned|p11|||See also p12.||||||13-DEC-06
19021|Utting Calcarenite|42547|4|Described|p102|||||||||
19021|Utting Calcarenite|42994|6|Mentioned|p13|||||||||
19021|Utting Calcarenite|43236|6|Mentioned|p14|Visean|Tournaisian|In the Bonaparte Basin.||||||13-DEC-06
19021|Utting Calcarenite|44994|6|Mentioned|p14|||||||||
19021|Utting Calcarenite|45038|14|Not recorded|p.111||Early Carboniferous|See also Figures. L.Carb.||||||
19021|Utting Calcarenite|45039|6|Mentioned|p1|||Lower Carboniferous. See also pp6,7,8,14 etc.||||||13-DEC-06
19021|Utting Calcarenite|45040|14|Not recorded|p7||Carboniferous|(?Carboniferous).||||||
19021|Utting Calcarenite|45050|6|Mentioned|p46|||Early Visean. See also p57.||||||13-DEC-06
19021|Utting Calcarenite|45063|6|Mentioned|p8|||See also p20 & 26 and Fig. 3.||||||13-DEC-06
19021|Utting Calcarenite|45097|5|Briefly described|p13|||See p19,21. Refers Bruce (1969). Conodonts. Chart.||||||13-DEC-06
19021|Utting Calcarenite|45169|4|Described|p6|||||||||
19021|Utting Calcarenite|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
19021|Utting Calcarenite|60364|4|Described|p189, 194|Visean|Visean|Conformably overlies Milligans Formation. Conformably overlain by Burvill Formation. Thickness: 120m. Open shelf carbonates. Richly fossiliferous including brachiopods, corals and trilobites. Ostracods described. Geological Province: Bonaparte Basin.||||||
19021|Utting Calcarenite|61542|4|Described|p276, p277 Fig. 2, p284|Visean|Visean|Of Weaber Gp. Overlies Yow Creek Fm (formerly mapped as Milligans Fm); parts underlie Kingfisher Shale and Burvill Fm.Geol.prov: Bonapart Basin/Petrel-Sub-basin.Fossiliferous sandy limestone, calcareous sandstone and minor fine-gr.sandstone; conodonts.||||||07-FEB-11
19021|Utting Calcarenite|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
19021|Utting Calcarenite|64694|6|Mentioned|p234 Fig.2, p238 Tb.1, p253|Visean|Visean|||Unit in Weaber Group.||Overlies Lower Milligans Formation. Is correlated with Upper Milligans Formation.||
19021|Utting Calcarenite|66498|6|Mentioned|p47-48|||Bonaparte Basin, WA.||Weaber Group.|||A highly fossiliferous unit (taxa described).|
19021|Utting Calcarenite|68297|5|Briefly described|p197|Visean|Visean|Bonaparte Basin. Includes shark faunas.||||||22-JAN-13
19021|Utting Calcarenite|69099|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
19021|Utting Calcarenite|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
19021|Utting Calcarenite|69452|3|Fully described|p36:9, 11-12, 14-16|Visean|Visean|Veevers and Roberts (1968). Petrel Sub-basin, Bonaparte Basin. Marine deposits. Type area is in Utting Gap (WA). Up to 120m thick. Offshore and onshore (subsurface). Also appears as Utting Conglomerate on 36:14.||Weaber Group.||Unconformably overlies Yow Creek or Milligans Formations. Lateral equivalent of Burvill Formation. Is overlain conformably by Kingfisher Shale.|Fossiliferous sandy limestone (wackestone and packstone), calcareous sandstone, minor fine- to medium-grained sandstone. Richly fossiliferous.|12-JUL-16
19021|Utting Calcarenite|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
19021|Utting Calcarenite|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Yow Creek Formation. Is overlain by Kingfisher Shale.||
19021|Utting Calcarenite|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||Overlies Yow Creek Formation, overlain by Kingfisher Shale|Fossiliferous sandy limestone, calcareous sandstone and sandstone.|
19021|Utting Calcarenite|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Visean|Visean|See also Regional geology: Fig.8, p11. Gas reservoir in Bonaparte 2.||Weaber Group.||Overlies Yow Creek Formation. Is overlain by Kingfisher Shale.||12-JUL-16
19021|Utting Calcarenite|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Yow Creek Formation. Overlain by Kingfisher Shale. Overlain by and equivalent to Burvill Formation.||
19036|Valentine Siltstone|22547|4|Described|p21|Orosirian|Orosirian|Of the Speewah Group. Geological province: Speewah Basin. Age: 1834 +/- 3 Ma. Thickness: 75 m. Overlies Tunganary Formation.||||||14-NOV-06
19036|Valentine Siltstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.||||||07-NOV-08
19036|Valentine Siltstone|23125|4|Described|Table.1, p389||Proterozoic|Age: Early Proterozoic. of Speewah Group.||||||
19036|Valentine Siltstone|23751|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Age: 1834+/-3 Ma. Of Speewah Group. Geological Province: Speewah Basin. Max. thickness: 70 m.||||||07-NOV-08
19036|Valentine Siltstone|29845|6|Mentioned|p113|||||||||
19036|Valentine Siltstone|30097|6|Mentioned|Table 23|||||||||
19036|Valentine Siltstone|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19036|Valentine Siltstone|30533|5|Briefly described|Table 2|||||||||
19036|Valentine Siltstone|30894|5|Briefly described|p250|||||||||
19036|Valentine Siltstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19036|Valentine Siltstone|30896|4|Described|p16|||||||||
19036|Valentine Siltstone|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19036|Valentine Siltstone|32660|5|Briefly described|Table 3|||||||||
19036|Valentine Siltstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
19036|Valentine Siltstone|32728|5|Briefly described|p34|||Mention Table 5||||||
19036|Valentine Siltstone|36551|6|Mentioned|Table 10|||||||||
19036|Valentine Siltstone|36885|4|Described|p186|||||||||
19036|Valentine Siltstone|37462|6|Mentioned|Fig.4.9|||||||||
19036|Valentine Siltstone|41557|6|Mentioned|p589|||||||||
19036|Valentine Siltstone|41987|5|Briefly described|Fig.4 P74|||||||||
19036|Valentine Siltstone|42149|6|Mentioned|Table 1 P709|||||||||
19036|Valentine Siltstone|42710|5|Briefly described|map legend|Proterozoic||||||||
19036|Valentine Siltstone|42811|5|Briefly described|p21|||of Speewah Group||||||
19036|Valentine Siltstone|43281|5|Briefly described|Map legend||Proterozoic|of Speewah Group.||||||
19036|Valentine Siltstone|43853|5|Briefly described|Map Legend||Proterozoic|||||||
19036|Valentine Siltstone|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
19036|Valentine Siltstone|44140|5|Briefly described|p295, p297 fig 4-4|Paleoproterozoic|Paleoproterozoic|80-360m thick.||Speewah Group|||Green chloritic siltstone, rhyolitic ashstone and tuff; ashstone is local marker.|
19036|Valentine Siltstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
19036|Valentine Siltstone|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Speewah Group.  Purple, grey and brown finely laminated shale and siltstone. Age: c.1835Ma. Geological Province: Speewah Basin.||||||07-NOV-08
19036|Valentine Siltstone|44317|4|Described|Table 2||Carpentarian|||||||
19036|Valentine Siltstone|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
19036|Valentine Siltstone|44363|5|Briefly described|p.6,11,12,13,15-28|||(Carpentarian), Speewah Group.||||||
19036|Valentine Siltstone|44364|14|Not recorded|map legend|||||||||
19036|Valentine Siltstone|44366|14|Not recorded|p.14, Table 2||Carpentarian|Part of Speewah Group.||||||
19036|Valentine Siltstone|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Speewah Group.||||||
19036|Valentine Siltstone|44397|14|Not recorded|p.17, Table 2||Carpentarian|Speewah Group.||||||
19036|Valentine Siltstone|44398|14|Not recorded|map legend||Carpentarian|||||||
19036|Valentine Siltstone|44868|5|Briefly described|Map Legend||Proterozoic|||||||
19036|Valentine Siltstone|45047|5|Briefly described|p28|||||||||
19036|Valentine Siltstone|48931|4|Described|p48|||||||||
19036|Valentine Siltstone|50437|6|Mentioned|p4.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Age: 1834 +/- 3Ma (Shrimp).||||||07-NOV-08
19036|Valentine Siltstone|60714|5|Briefly described|p113. |Orosirian|Orosirian|Age from interbedded felsic volcanic rocks.|1834 +/- 3 Ma (U-Pb zircon: Page and Sun 1994).|Of the Speewah Group.||Overlies Tunganary Formation. Is overlain by Valentine Siltstone.|Sediments and interbedded felsic volcanic rocks.|
19036|Valentine Siltstone|60724|6|Mentioned|p17|||On LANSDOWNE sheet. Age: 1.83Ga.||||||
19036|Valentine Siltstone|63866|5|Briefly described|p133, p137|Orosirian|Orosirian|Western Zone, Halls Creek Orogen.|c. 1835 Ma (Page and Sun, 1994)|Speewah Group||||
19036|Valentine Siltstone|64748|4|Described|p268, p269 Fig 2||Orosirian|Felsic volcanic rocks; of the Speewah Group; max U-Pb zircon age 1834+/-3Ma; Underlies the Lansdowne Arkose; overlies the Tunganary Formation||||||08-MAY-15
19036|Valentine Siltstone|67563|5|Briefly described|p121, p122 Fig.2|Orosirian|Orosirian|SHRIMP U-Pb zircon age (Page and Sun 1994).|1834 +/- 3 Ma|Of the Speewah Group.||||20-JAN-17
19036|Valentine Siltstone|68078|4|Described|p5-6, p8, p11, p14 figure 10, p23-24|Paleoproterozoic|Paleoproterozoic|Age is of felsic volcanic rocks.|1835 +/- 3 Ma (SHRIMP)|Speewah Group||Overlies Lansdowne Arkose, Overlain by Bedford Sandstone|Siltstone, thin beds of dacite to rhyolite and volcaniclastic siltstone, base marked by crystal poor rhyolite.|13-SEP-22
19036|Valentine Siltstone|68992|5|Briefly described|p498 Fig.1, p499|Orosirian|Orosirian|Speewah Basin. Called Valentine Siltstone Formation on p499. Geochronology determined from a felsic volcanic tuff bed. Magmatic zircon age.|1834 +/- 3 Ma (Page and Sun, 1994).|Of the Speewah Group.||||
19036|Valentine Siltstone|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|||Speewah Group.||Overlies Tunganary Formation. Is overlain by Lansdowne Arkose.||
19036|Valentine Siltstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Speewah Basin. Data from OZCHRON1. Comment: 'This zircon igneous crystallisation age is a good depositional age for the sequence. The ~1800 Ma age for the intrusive Hart Dolerite is consistent with this result,ie intruded by He'. Unit relationships from geochron file 182106.1.pdf.|1834+/-3 Ma U/Pb SHRIMP|Speewah Group||Conformably overlain by Lansdowne Arkose.|Flaggy siltstone and mudstone, commonly micaceous or chloritic; minor, thin-bedded, feldspathic quartz sandstone and dacitic to rhyolitic, volcaniclastic siltstone|21-JUL-15
19036|Valentine Siltstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1834 Ma|Speewah Group|||Flaggy, siltstone and mudstone, commonly micaceous or chloritic; minor thin bedded feldspathic quartz sandstone and dacitic to rhyloitic volcaniclastic siltstone.|
19036|Valentine Siltstone|69585|5|Briefly described|p4-5|Orosirian|Orosirian|Western Lamboo Province. Age from a felsic volcaniclastic component; indicates that deposition of Speewah Group was synchronous with the Halls Creek Orogeny.|1835 +/- 3 Ma (Page and Sun, 1994).|Speewah Group.||Conformably overlies Tunganary Formation. Is overlain conformably by Landsowne Arkose.||
19036|Valentine Siltstone|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Speewah Basin. Intruded by a felsic volcanic unit dates at 1834+\-3 Ma (Griffin et al., 1993). Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_interpgeol_lut.csv and geochron files.|1834+\-3 Ma (Isotopic)|Unit of Speewah Group.||Overlain conformably by Landsdowne Arkose.|Flaggy siltstone and mudstone, commonly micaceous or chloritic; minor, thin-bedded, feldspathic quartz sandstone and dacitic to rhyolitic, volcaniclastic siltstone|
19036|Valentine Siltstone|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin, Kimberley Craton.|c.1835 Ma; Page and Sun (1994).|Unit in Speewah Group.|||Flaggy siltstone and mudstone, commonly micaceous or chloritic; minor, thin-bedded, feldspathic quartz sandstone and dacitic to rhyolitic volcaniclastic siltstone.|
19036|Valentine Siltstone|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Speewah Basin; North Australian Craton.|c.1835 Ma (Sheppard et al., 2012).|Speewah Group.||Overlies Tunganary Formation. Is overlain by Lansdowne Arkose.|Flaggy siltstone and mudstone, commonly micaceous or chloritic; minor, thin-bedded, feldspathic quartz sandstone and dacitic to rhyolitic, volcaniclastic siltstone.|
19036|Valentine Siltstone|70154|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv.|1835 Ma|Speewah Group||||
19036|Valentine Siltstone|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, 1m_geologyl12_lithology_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 1m_geologyl12_lut.csv and geochron files.|1835+\-3 Ma (isotopic)|Unit of Speewah Group.||Overlain conformably by Lansdowne Arkose. Underlain conformably by Tunganary Formation.|Poorly exposed dark grey-green tuff and tuffaceous siltstone with conchoidal fracture surfaces, overlain by grey-green flaggy laminated siltstone grading up into fine feldspathic sandstone|
19036|Valentine Siltstone|71281|4|Described|p421-425, p429-432|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Speewah Basin. Up to 75m thick. Swampy flood-plain deposits. Depositional age from a correlated volcaniclastic rock; this conclusion is challenged: the age may be of maximum deposition. Photo and photomicrograph.|1835 +/- 3 Ma (Sheppard et al., 2012).|Speewah Group.||Conformably overlies Tunganary Formation. Is overlain conformably by Lansdowne Arkose. Is intruded extensively by Hart Dolerite.|Dark grey-green tuff and tuffaceous siltstone with conchoidal fracture surfaces, grey-green flaggy laminated siltstone and fine feldspathic sandstone; chloritic laminae. Contains a 1-2m thick marker interval rich in felsic volcaniclastic fragments.|
19036|Valentine Siltstone|71784|6|Mentioned|p83-84||Proterozoic|Speewah Group.||||||
19036|Valentine Siltstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Speewah Group.|||Flaggy siltstone and mudstone, commonly micaceous or chloritic; minor thin-bedded feldspathic and quartz sandstone.|
19036|Valentine Siltstone|72437|5|Briefly described|p12, p113|Palaeoproterozoic|Palaeoproterozoic|A black crystal-poor rhyolite tuff which marks the base was dated by Page and Sun (1994).|1834 +/- 3 Ma|Speewah Group|||Siltstone with some thin interbeds of dacite to rhyolite tuff.|
19036|Valentine Siltstone|72490|5|Briefly described|p3-6, p10-11, p13|||Maximum thickness of 75 m. Zircons dated at 1835 +/- 3 Ma in volcaniclastic rock were proposed as reflecting a xenocrystic component.||Speewah Group|||Dark grey-green tuff and tuffaceous siltstone with conchoidal fracture surfaces, grey-green flaggy laminated siltstone and fine feldspathic sandstone.|
19044|Van Diemen Sandstone|24047|5|Briefly described|p13, p85|Tertiary|Tertiary|Geological Province: Money Shoal Basin.||||||
19044|Van Diemen Sandstone|31406|4|Described|Table 2|||Mention p4.||||||13-DEC-06
19044|Van Diemen Sandstone|31407|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
19044|Van Diemen Sandstone|31408|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|31409|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|31410|2|Defined|p10|Cenozoic|Cenozoic|||||||19-NOV-08
19044|Van Diemen Sandstone|32472|6|Mentioned|p3|||||||||
19044|Van Diemen Sandstone|41532|6|Mentioned|Fig.15|||||||||
19044|Van Diemen Sandstone|42442|6|Mentioned|Fig.3 P4 P5|||||||||
19044|Van Diemen Sandstone|45121|2|Defined|p51|Tertiary|Tertiary|||||||
19044|Van Diemen Sandstone|45168|6|Mentioned|p12|||||||||
19044|Van Diemen Sandstone|46902|6|Mentioned|p39|||||||||
19044|Van Diemen Sandstone|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Max. thickness: 250m. Geological Province: Money Shoal Basin - north and south.||||||
19044|Van Diemen Sandstone|69456|4|Described|p40:2; 40:3 Fig.40.4; 40:4, 6, 8-9, 12|Eocene|Eocene|See also 40:15 Fig.40.16. Hughes and Senior (1974); Hughes (1978). Money Shoal Basin. Ungrouped. Less than 60m thick. Fluvial deposits. Widely exposed as sea cliffs, discontinuous low ridges and dissected plateaux. Paleogene units "of equivalent age" to this Sandstone occur in the Woodbine Group of the Bonaparte Basin. Source of heavy mineral sands deposits (Tiwi Islands). Hosts lateritic bauxite.||||Unconformably overlies onshore Bathurst Island Group (Moonkinu Sandstone). ?Is overlain unconformably by Woodbine Group.|White to yellow, cross-bedded, medium- to coarse-grained quartz sandstone, minor lenses of siltstone, mudstone (with plant fossils) and granular conglomerate. Inland exposures are strongly weathered and iron-stained.|12-JUL-16
19044|Van Diemen Sandstone|69458|6|Mentioned|p42:6|Neogene|Paleogene|Money Shoal Basin.||||||12-JUL-16
19044|Van Diemen Sandstone|69673|6|Mentioned|p204|Cretaceous|Cretaceous||||||Cross bedded, medium to coarse grained quartz sandstone with minor lenses of siltstone and granular conglomerate.|
19044|Van Diemen Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
19070|Vee Formation|5952|6|Mentioned|p222|||Defined by Mory (1988).||||||05-MAY-09
19070|Vee Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Campanian|Cenomanian|100-250m thick open marine shelf deposits. Type section: Swift 1 (2140-2360m).||Bathurst Island Group||Grades into Brown Gannet Limestone. Coeval with Wangarlu Formation to eat. Overlain by Turnstone Formation.|Marl, calcilutite, calcareous claystone.|
19070|Vee Formation|23377|6|Mentioned|p212 Fig.5||Late Cretaceous|In the Vulcan Sub-basin..||||||13-DEC-06
19070|Vee Formation|41459|6|Mentioned|Fig.2|||||||||
19070|Vee Formation|41532|2|Defined|p306|Late Cretaceous||||||||
19070|Vee Formation|41731|6|Mentioned|Fig.3|||||||||
19070|Vee Formation|42442|2|Defined|p29|early Campanian|Cenomanian|Age: Late Cretaceous (Cenomanian to early Campanian).||||||13-DEC-06
19070|Vee Formation|43661|6|Mentioned|Fig.3|||||||||
19070|Vee Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
19070|Vee Formation|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
19070|Vee Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
19076|Venture Slate Member|30562|4|Described|p40|||Refers Hall & Bekker (1965). See also P37||||||
19076|Venture Slate Member|43162|6|Mentioned|6|||||||||
19096|Victoria Plateau Sandstone|23172|4|Described|Map Legend|||||||||
19096|Victoria Plateau Sandstone|23816|4|Described|p253|Pleistocene|Eocene|Formerly known as the "Plateau Beds" or "Victoria Plateau Beds". Geological Province: Perth Basin. Max. thickness: 20 m.||||||27-APR-05
19096|Victoria Plateau Sandstone|30973|6|Mentioned|Map legend|Tertiary|Tertiary|Prob. Tertiary||||||
19096|Victoria Plateau Sandstone|32337|4|Described|p25|||||||||
19096|Victoria Plateau Sandstone|36293|2|Defined|p202|late Eocene|late Eocene|Prob.Upper Eocene||||||
19096|Victoria Plateau Sandstone|36890|3|Fully described|p253|||Formerly Victoria Plateau Beds||||||
19096|Victoria Plateau Sandstone|37298|6|Mentioned|p91|||||||||
19096|Victoria Plateau Sandstone|40340|6|Mentioned|Table 2|||||||||
19096|Victoria Plateau Sandstone|40346|6|Mentioned|Map legend|Cenozoic|Cenozoic|Prob. Cainozoic||||||19-NOV-08
19096|Victoria Plateau Sandstone|40794|6|Mentioned|p95|||||||||
19096|Victoria Plateau Sandstone|44144|4|Described|p502 Tb.4-21, p519|Miocene|Miocene|Type Section: High Cliff; 29o56'40''S 115o32'45''E. 20m thick fluvial deposits, including wood fragments.||||Correlates with Pindilya Formation.|Poorly sorted, usually fine-grained sandstone; lesser siltstone and conglomerate.|
19096|Victoria Plateau Sandstone|61811|5|Briefly described|p40 Fig.43, p65.|?Late Eocene|?Late Eocene|Type section details in Appendix 1.||||Unconformably overlies Irwin River Coal Measures.|Sandstone; lesser shale; minor conglomerate.|
19096|Victoria Plateau Sandstone|64635|6|Mentioned|p21 Fig.18|||||||Unconformably overlies Irwin River Coal Measures.||
19096|Victoria Plateau Sandstone|70097|5|Briefly described|p20 Fig.4|Rupelian|Priabonian|Northern Perth Basin. Irwin Terrace.||||Overlies Wagina Sandstone.|Sandstone.|12-SEP-17
19132|Violet Valley Tonalite|22547|4|Described|p18||Orosirian|Of the Sally Downs supersuite. Much of it previously assigned to Mabel Downs Tonalite.||||||14-NOV-06
19132|Violet Valley Tonalite|22741|6|Mentioned|P20|||||||||
19132|Violet Valley Tonalite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
19132|Violet Valley Tonalite|23751|4|Described|p18|||Massive to weakly foliated, medium-grained biotite (-hornblende) granodiorite and tonalite. Of Kevins Dam suite.||||||
19132|Violet Valley 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
19132|Violet Valley 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
19132|Violet Valley Tonalite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19132|Violet Valley Tonalite|32728|6|Mentioned|Table 4|||||||||
19132|Violet Valley Tonalite|36885|4|Described|p175|||||||||
19132|Violet Valley Tonalite|41977|6|Mentioned|p471|||||||||
19132|Violet Valley Tonalite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
19132|Violet Valley Tonalite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
19132|Violet Valley Tonalite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
19132|Violet Valley Tonalite|44155|4|Described|p242 Tb.3-5, p248 Tb.3-8|||East Kimberley.||Lamboo Complex||Intrudes Bow River Granite.|Biotite tonalite; some granodiorite and gabbro.|
19132|Violet Valley Tonalite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
19132|Violet Valley Tonalite|44317|5|Briefly described|Table 1||Proterozoic|||||||
19132|Violet Valley Tonalite|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
19132|Violet Valley Tonalite|44363|5|Briefly described|p.7,9||Paleoproterozoic|Lower Proterozoic, Lamboo Complex.||||||07-NOV-08
19132|Violet Valley Tonalite|44364|14|Not recorded|map legend|||||||||
19132|Violet Valley Tonalite|44366|14|Not recorded|p.10, Table 1||Proterozoic|||||||
19132|Violet Valley Tonalite|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Lamboo Complex.||||||
19132|Violet Valley Tonalite|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
19132|Violet Valley Tonalite|44398|14|Not recorded|map legend||Proterozoic|||||||
19132|Violet Valley Tonalite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
19132|Violet Valley Tonalite|45047|4|Described|p13|||See also P26. Lamboo Complex.||||||12-AUG-08
19132|Violet Valley Tonalite|45048|3|Fully described|p66|||Carpentarian or Lower Proterozoic||||||
19132|Violet Valley Tonalite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sally Downs Supersuite. Used interchangeably with Violet Valley Granodiorite.||||||07-NOV-08
19132|Violet Valley Tonalite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen.||Kevins Dam Suite|Includes unnamed subdivision.||Biotite-hornblende metatonalite and biotite metagranodiorite; fine to medium grained; weakly porphyritic; massive to foliated.|04-AUG-15
19132|Violet Valley Tonalite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kevins Dam Suite|||Biotite metagranodiorite and biotite-hornblende metatonalite; fine to medium grained; weakly porphyritic, massive to foliated.|
19132|Violet Valley 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.|1827-1808 Ma (Inferred)|Unit of Kevins Dam Suite.|||Biotite-hornblende metatonalite and biotite metagranodiorite; fine to medium grained; weakly porphyritic; massive to foliated|
19132|Violet Valley Tonalite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1808-1827 Ma|Kevins Dam Suite|||Biotite--hornblende metatonalite and biotite metagranodiorite; fine to medium grained; weakly porphyritic; massive to foliated. Medium grained, weakly porphyritic biotite metagranodiorite.|
19132|Violet Valley 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.|1827-1808 Ma (inferred)|Unit of Kevins Dam Suite.|||Biotite-hornblende metatonalite and biotite metagranodiorite; fine to medium grained; weakly porphyritic; massive to foliated|
19132|Violet Valley Tonalite|72437|5|Briefly described|p107-108|||Whole rock analyses are provided.||Kevins Dam Suite|||Foliated biotite tonalite, biotite tonalite, foliated biotite granodiorite, biotite-quartz monzonite.|
19137|Virgin Hills Formation|22550|6|Mentioned|p 20, Fig 3|||||||||
19137|Virgin Hills Formation|22741|5|Briefly described|P21, P23, Table3 P16|Famennian|Frasnian|||||||
19137|Virgin Hills Formation|22767|6|Mentioned|P20|||Resembles the Babrongan Beds||||||
19137|Virgin Hills Formation|22776|6|Mentioned|p17|||Probably equivalent of Babrongan Beds.||||||
19137|Virgin Hills Formation|23338|5|Briefly described|915 Fig.3|Famennian|Famennian|||||||
19137|Virgin Hills Formation|23847|5|Briefly described|p296|Famennian|Frasnian|Geological Province: Canning Basin.||||||
19137|Virgin Hills Formation|23903|5|Briefly described|p1597 Fig.2|Famennian|Frasnian|Geological Province: Canning Basin.||||||10-NOV-08
19137|Virgin Hills Formation|24000|5|Briefly described|p348 Fig. 2|Famennian|Frasnian|Geological Province: Canning Basin.||||||
19137|Virgin Hills Formation|24061|5|Briefly described|p180|Middle Devonian|Middle Devonian|Of "Lennard River Group"?  Geological Province:  Canning Basin.||||||
19137|Virgin Hills Formation|24503|5|Briefly described|Map legend|Devonian|Devonian|Geological Province: Canning Basin.||||||
19137|Virgin Hills Formation|30187|6|Mentioned|p179|||||||||
19137|Virgin Hills Formation|31152|6|Mentioned|p2|||||||||
19137|Virgin Hills Formation|31332|6|Mentioned|Fig. 3|||||||||
19137|Virgin Hills Formation|31661|6|Mentioned|p653|||M.Devonian||||||
19137|Virgin Hills Formation|31870|6|Mentioned|p8|||||||||
19137|Virgin Hills Formation|32594|4|Described|p3|||Refers fossil content||||||
19137|Virgin Hills Formation|32603|6|Mentioned|p99|||||||||
19137|Virgin Hills Formation|32617|6|Mentioned|p33|||See also P35||||||
19137|Virgin Hills Formation|32647|6|Mentioned|p98|||||||||
19137|Virgin Hills Formation|32865|6|Mentioned|p472|||Frasnian||||||
19137|Virgin Hills Formation|33042|6|Mentioned|p723|||See also PP725-735,739 etc.||||||
19137|Virgin Hills Formation|33112|6|Mentioned|p179|||Devonian||||||
19137|Virgin Hills Formation|34154|6|Mentioned|p77|||Devonian||||||
19137|Virgin Hills Formation|34427|6|Mentioned|Fig.3|||||||||
19137|Virgin Hills Formation|34428|6|Mentioned|p1008|||See also P1009,1010. Upper Devonian.||||||
19137|Virgin Hills Formation|34484|6|Mentioned|p21|||||||||
19137|Virgin Hills Formation|35104|6|Mentioned|p5|||||||||
19137|Virgin Hills Formation|36257|6|Mentioned|Table 2.1|||||||||
19137|Virgin Hills Formation|36365|6|Mentioned|Fig.8|||||||||
19137|Virgin Hills Formation|36890|3|Fully described|p333|||||||||
19137|Virgin Hills Formation|38009|6|Mentioned|p177|||||||||
19137|Virgin Hills Formation|38207|6|Mentioned|p161|||||||||
19137|Virgin Hills Formation|39702|6|Mentioned|Fig.2|||||||||
19137|Virgin Hills Formation|40236|6|Mentioned|p131|||||||||
19137|Virgin Hills Formation|40797|6|Mentioned|p155|||||||||
19137|Virgin Hills Formation|41111|6|Mentioned|p509|||||||||
19137|Virgin Hills Formation|41113|6|Mentioned|p519|||||||||
19137|Virgin Hills Formation|41139|6|Mentioned|Fig.2|||||||||
19137|Virgin Hills Formation|41169|6|Mentioned|p145|||||||||
19137|Virgin Hills Formation|41215|5|Briefly described|p277|||||||||
19137|Virgin Hills Formation|41828|6|Mentioned|Table 1|||||||||
19137|Virgin Hills Formation|41894|4|Described|p4|||||||||
19137|Virgin Hills Formation|42030|5|Briefly described|p747|||||||||
19137|Virgin Hills Formation|42073|5|Briefly described|p291|||||||||
19137|Virgin Hills Formation|42080|6|Mentioned|p281|||||||||
19137|Virgin Hills Formation|42111|5|Briefly described|p88|||See also Text fig.4||||||
19137|Virgin Hills Formation|42176|6|Mentioned|p204|||||||||
19137|Virgin Hills Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
19137|Virgin Hills Formation|42351|5|Briefly described|Fig.4 P41|||||||||
19137|Virgin Hills Formation|42473|6|Mentioned|p85|||||||||
19137|Virgin Hills Formation|42564|5|Briefly described|p10|||See also "Virgin Hills Formation" of Billiton which is equivalent to Lower Napier Formation.||||||13-NOV-07
19137|Virgin Hills Formation|42860|5|Briefly described|Fig.2|||||||||
19137|Virgin Hills Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
19137|Virgin Hills Formation|42930|5|Briefly described|Fig.1 p473|Late Devonian|Devonian|Geological Province: Canning Basin. Conformable over Gogo Shale. Geological Province: Canning Basin.||||||10-NOV-08
19137|Virgin Hills Formation|42933|5|Briefly described|Fig.94 p258|||Actually listed as just Virgin Hills.||||||
19137|Virgin Hills Formation|43173|6|Mentioned|54||Late Devonian|||||||
19137|Virgin Hills Formation|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
19137|Virgin Hills Formation|43723|6|Mentioned|p53||Devonian|||||||
19137|Virgin Hills Formation|43815|6|Mentioned|Table 1,p95-96|||||||||
19137|Virgin Hills Formation|44143|4|Described|p438 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 600m thick; siltstone, shale, calcarenite, calcilutite, calcirudite, and megabreccia; shallow marine. Interfingers with Windjana and Pillara Limestones. Type section about 8km N of Mount Pierre (NOONKANBAH: 18deg 16' 30" S, 25deg 52' 00" E). Contains conodonts and ammonoids; middle Frasnian to middle Famennian.||||||24-NOV-17
19137|Virgin Hills Formation|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Fore-reef subfacies and basin facies; calcarenite, limestone breccia and megabreccia, siltstone, snadstone and minor conglomerate; characteristically red in colour; includes calcareous sandstone in Sparke Range area. geol.Prov: Canning Basin.||||||19-MAY-05
19137|Virgin Hills Formation|44397|14|Not recorded|p.12,Figs.2,3,Tb.4|||Famennian to Frasnian.||||||
19137|Virgin Hills Formation|44398|14|Not recorded|map legend|||Famennian to Frasnian.||||||
19137|Virgin Hills Formation|44403|2|Defined|opp.p.6, Tb.1||Famennian|E/51-12, part of the Mt.Pierre Group silty limestone, calcareous siltstone, shale, small bioherms sandy and conglomeratic facies. Frasnian and Famennian, corals, goniatites. U/lain conformably by Gogo Formation, unconf. Pillara Fm.O/lain by Fairfield Beds||||||
19137|Virgin Hills Formation|44998|14|Not recorded|p41||Late Devonian|U.Devonian. On many pages. p.25,36,42. See also App.3 p279.||||||
19137|Virgin Hills Formation|45039|6|Mentioned|p21|||Upper Devonian.||||||
19137|Virgin Hills Formation|45041|6|Mentioned|Fig.45|||||||||
19137|Virgin Hills Formation|45063|6|Mentioned|Fig. 9|||||||||
19137|Virgin Hills Formation|45101|5|Briefly described|p6|||See also p21. Conodont content||||||13-NOV-07
19137|Virgin Hills Formation|45133|6|Mentioned|p4|||||||||
19137|Virgin Hills Formation|45143|3|Fully described|Fig.3|||Time-stratigraphic interpretations.||||||
19137|Virgin Hills Formation|45153|2|Defined|App.3-54|Late Devonian|Late Devonian|See also App.3-38.||||||13-NOV-07
19137|Virgin Hills Formation|45158|4|Described|p24|||||||||
19137|Virgin Hills Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
19137|Virgin Hills Formation|48573|14|Not recorded|p.17.|||(E51-7/Alexander Creek)||||||
19137|Virgin Hills Formation|48831|14|Not recorded|p.81,83-85|||||||||
19137|Virgin Hills Formation|48837|2|Defined|p.25-28|||On many pages. p.18,25-28,35,39. Conformably overlies Gogo Formation. Unconformably overlain Fairfield Beds.||||||13-NOV-07
19137|Virgin Hills Formation|48848|14|Not recorded|p.34,39,69,78,92,95|||||||||
19137|Virgin Hills Formation|48925|6|Mentioned|p31|||Upper Devonian age. Fauna in||||||
19137|Virgin Hills Formation|50150|5|Briefly described|p9|Famennian|Famennian|Geological Province: Canning Basin.||||||
19137|Virgin Hills Formation|62735|4|Described|p981, p982, p983 Fig. 2|Famennian|Frasnian|Very fine-gr.calcarenites/calcilutites, thinly bedded; commonly hematite-rich; forereef facies with trilobite-bearing horizons in McWhae Ridge and Bugle Gap areas. Contains several informally named horizons. O'lies Pillara Fm. Geol.Prov: Canning Basin.||||||04-OCT-06
19137|Virgin Hills Formation|63938|5|Briefly described|p49 Fig.1, p50 Fig.2|Famennian|Frasnian|Marginal slope & basin.||||||10-NOV-08
19137|Virgin Hills Formation|64159|5|Briefly described|p91 Fig. 6|Famennian|Famennian|Part of the Lennard Reef facies development. Mainly a siltstone unit.||||||
19137|Virgin Hills Formation|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Underlain by Gogo Formation and unconformably by Napier Formation, overlain by Clanmeyer Fm and Windjana Limestone. Limestone, sandstone (shallow marine - marine). Geological Province: Canning Basin.||||||08-FEB-10
19137|Virgin Hills Formation|64502|5|Briefly described|p764, p765 Fig. 2|Famennian|Frasnian|||||||
19137|Virgin Hills 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.||||||10-NOV-08
19137|Virgin Hills Formation|64643|5|Briefly described|p7 Fig. 5, p34, 35 |Famennian|Frasnian|Marginal slope facies||||||
19137|Virgin Hills Formation|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19137|Virgin Hills Formation|65486|5|Briefly described|p6-7,9,48,53,72; Figs.5,6,7,72; Plate 1.|Famennian|Frasnian|Marginal-slope and basin limestone, sandstone and siltstone, Canning Basin. Overlies Napier Formation, Gogo Formation, Sadler Limestone. Underlies Piker Hills Formation, underlies and interfingers with Windjana Limestone.||||||
19137|Virgin Hills Formation|66127|3|Fully described|pp19-21, pp54-57, pp283-286, p288.|Middle Famennian|Early Frasnian|Named after the Virgin Hills on Gogo Station. Type section is east of Needle Eye Rocks. Richly fossiliferous. Maximum thickness probably >750 m. Well-developed tepee structures and symmetrical ripple marks. Shown on Plates 3, 4, 5, 7, 8.|||Includes Lower and Upper Beloceras Beds.|Overlies Gogo Formation, Sadler Limestone and, unconformably, Pillara Limestone. Interfingers with Bugle Gap Limestone. Underlies Piker Hills Formation conformably.|Basin facies: bright red, thin-bedded calcareous siltstone and shale; interbedded with limestone, sandstone, minor conglomerate. Marginal-slope facies: red calcarenites and thick-bedded debris-flow breccias.|
19137|Virgin Hills Formation|67131|6|Mentioned|p3 Fig. 2,|Famennian|Frasnian|Marginal-slope and basin facies.||||Overlies Gogo Formation, Sadler Limestone. Overlain by Piker Hills Formation, Bugle Gap Limestone.||
19137|Virgin Hills Formation|68297|5|Briefly described|p194|Famennian|Famennian|Canning Basin. Marginifera zone.||||||
19137|Virgin Hills Formation|69099|6|Mentioned|500k_geologyp08_lut.csv|Fammenian||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.||||||04-AUG-15
19137|Virgin Hills Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
19137|Virgin Hills Formation|69182|6|Mentioned|Ch4 p64, Ch4 p87|||Deposited in a marine envrionment as part of a turbidite sequence.|||||Clastic sedimentary rocks with calcareous clasts from shelfal limestones.|
19137|Virgin Hills Formation|69312|6|Mentioned|p19|Devonian|Devonian|Canning Basin.||||Overlies the Windjana Limestone. Overlain by the Pillara Limestone.||
19137|Virgin Hills Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Mount House Group.|||Fossiliferous, commonly red, shallow marine reef complex marginal slope and basin facies, interbedded calcareous siltstone, shale, sandstone, calcarenite, calcilutite; large blocks of reef common forming mega-breccia in places|
19137|Virgin Hills Formation|71811|5|Briefly described|Map legend.|Famennian|Frasnian|Canning Basin. A unit in the Devonian Reef Complexes: Frasnian and Famennian marginal slope and basin facies.|||||Thin-bedded red and grey silty limestone, siltstone, sandstone, and calcirudite (in debris flows) with some allochthonous blocks of reef limestone.|06-MAY-19
19137|Virgin Hills Formation|72502|6|Mentioned|p5, p21|Famennian|Frasnian|Lennard Shelf, Canning Basin. Shark fauna are similar to the Jalodus biofacies type [of Ginter, 2000]. Includes upper to distal slope facies.||||Underlain by Gogo Formation, Sadler Limestone. Overlain by Piker Hills Formation. Overlain and equivalent to Bugle Gap Formation. Equivalent to Napier Formation, Windjana Limestone, Pillara Limestone.||
19148|Vulcan Formation|5952|5|Briefly described|p215 Fig. 5|||Appears as Vulcan in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
19148|Vulcan Formation|23377|5|Briefly described|p223||Late Jurassic|In the Vulcan Sub-basin.||||||13-DEC-06
19148|Vulcan Formation|23378|5|Briefly described|p197,202|Early Cretaceous|Late Jurassic|In the Vulcan Sub-basin.||||||01-MAR-10
19148|Vulcan Formation|42053|4|Described|p42|||||||||01-MAR-10
19148|Vulcan Formation|42861|6|Mentioned|p4|||||||||
19148|Vulcan Formation|43826|6|Mentioned|Fig.2,p163|Early Cretaceous|Late Jurassic|||||||01-MAR-10
19148|Vulcan Formation|60378|6|Mentioned|p95|Late Jurassic|Late Jurassic|Includes interpreted deep marine fan sediments considered to be a reservoir facies.|||See also informal subdivisions: Lower Vulcan Formation, Upper Vulcan Formation.|||
19148|Vulcan Formation|61550|6|Mentioned|p494, p495 Fig.2. |Late Jurassic|Late Jurassic|Contains marine hydrocarbon source rocks.||Unit in Swan Group.||Overlies Montara Formation. Is overlain unconformably by Echuca Shoals Formation.||
19148|Vulcan Formation|64697|5|Briefly described|p84 Fig.2, p86, p87, p88, p91 |Early Cretaceous|Late Jurassic|||||||
19148|Vulcan Formation|65078|5|Briefly described|p35|Triassic|Triassic|Includes a clastic "basal transgressive sand" in both Lower Vulcan and Upper Vulcan Formations. Geological province: Vulcan Sub-basin.||||||05-MAY-09
19148|Vulcan Formation|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Middle Jurassic|Browse Basin.||||Overlies Montara Formation.||15-SEP-17
19148|Vulcan Formation|69452|5|Briefly described|p36:15|Early Cretaceous|Jurassic|Bonaparte Basin.||Swan Group.||||12-JUL-16
19148|Vulcan Formation|70061|5|Briefly described|Regional geology; p6, p10, p12-13, p17|Late Jurassic|Middle Jurassic|See also Vulcan: p1-3. Gas- and oil-prone source rocks produce all produced oils in the Vulcan Sub-basin. Forms a widespread, competent seal across the Vulcan Sub-basin. Potential gas reservoir in Vulcan Sub-basin.|||||Marine sediments including mudstones and submarine fan sandstones.|12-JUL-16
19148|Vulcan Formation|70064|5|Briefly described|Regional p4-8, p10. Central: p1-2|Valanginian|Callovian|See also Northern: p1-2. Yampi: p1-2. Contains organic-rich rocks with fair to moderate oil potential. Potential reservoirs in horsts and tilted fault-blocks. Is a potential regional seal.|||||Interbedded sandstones and shales.|12-JUL-16
19171|Wabco Shale|22484|5|Briefly described|p83 Fig13|||of the Mount Minnie Group||||||
19171|Wabco Shale|23325|5|Briefly described|map legend|Proterozoic|Proterozoic|of Mount Minnie Group||||||
19171|Wabco Shale|24544|4|Described|p48|Paleoproterozoic|Paleoproterozoic|Of Mount Minnie Group. Mudstone with thin interbeds of quartz sandstone. Geological Province: Ashburton Province.||||||07-NOV-08
19171|Wabco Shale|34066|4|Described|p9|||Mid.Prot.||||||
19171|Wabco Shale|36883|4|Described|p146|||||||||
19171|Wabco Shale|37460|6|Mentioned|p157|||||||||
19171|Wabco Shale|42260|4|Described|p99|||||||||
19171|Wabco Shale|44477|4|Described|p.13, Table 1||Proterozoic|SF/50-6.||||||
19171|Wabco Shale|44478|14|Not recorded|map legend||Proterozoic|||||||
19171|Wabco Shale|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
19171|Wabco Shale|67855|5|Briefly described|p221|||Up to 500m thick but absent from Parry Range.||Mount Minnie Group||Overlies Brodagee Sandstone (conformably).|Mudstone and thin-bedded quartz sandstone.|
19171|Wabco Shale|69028|5|Briefly described|Map Legend|Statherian|Statherian|Ashburton and Blair Basins.  Mapped with Brodagee and Warramboo Sandstones as a single unit.||Of the Mount Minnie Group.|||Quartz sandstone, conglomerate, siltstone and mudstone.|07-MAY-14
19171|Wabco Shale|72758|5|Briefly described|p10 Tb.1, p48-49.|||500 m thick. Marine shelf deposits.||Mount Minnie Group||Conformably overlies Brodagee Sandstone and conformably underlies Warramboo Sandstone.|Mudstone and thin beds of sandstone.|
19179|Wadera Member|24455|5|Briefly described|p327|||Of the Cardabia Calcarenite. Geological Province: Carnarvon Basin.||||||22-MAR-05
19179|Wadera Member|40617|6|Mentioned|p14|||||||||
19179|Wadera Member|41271|4|Described|p166|||||||||
19179|Wadera Member|61155|5|Briefly described|p15|Late Paleocene|Late Paleocene|Of the Cardabia Calcarenite. Geological Province: Carnarvon Basin/onshore.||||||13-SEP-05
19180|Wadgingarra Gabbro|32337|4|Described|p9|||||||||
19180|Wadgingarra Gabbro|41594|4|Described|p65|||||||||
19180|Wadgingarra Gabbro|70226|5|Briefly described|Map legend.|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. The four minor facies are mapped separately.||Warriedar Suite.|||Massive gabbro with granophyric leucogabbro towards the top of the intrusion; metamorphosed. Also dolerite, leucograbbro, tremolite-chlorite(-talc) schist, and peridotite.|16-DEC-15
19180|Wadgingarra Gabbro|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. Numerous additional lithologies are discussed.|ca 28012793 Ma (inferred)|Warriedar Suite|||Peridotite; fine to medium grained; commonly serpentinized. Massive gabbro with granophyric leucogabbro towards the top of the intrusion; metamorphosed. Dolerite; minor gabbro and basalt, leucogabbro, metamorphosed. Tremolitechloritetalc chist.|
19180|Wadgingarra Gabbro|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
19180|Wadgingarra 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, 1m_geologyp12_lut.csv.|2801-2793 Ma (inferred)|Unit of Warriedar Suite.|||Dolerite; minor gabbro and basalt; massive to weakly deformed, and metamorphosed; dolerite; minor gabbro and basalt; massive to weakly deformed, and metamorphosed; tremolite-chlorite(-talc) schist; strongly sheared|
19225|Waldecks Member|40837|6|Mentioned|p260|||||||||
19225|Waldecks Member|43599|6|Mentioned|p248|||||||||
19225|Waldecks Member|64643|5|Briefly described|p3 Fig. 2|Pridoli|Wenlock|Of Worral Formation?||||||
19225|Waldecks Member|65449|3|Fully described|p1, p6, p8-9, p29, p31-34, p39 Fig.20|Pridoli|Llandovery|See also p51-53; Plates 1-4, 9-11. Lehmann (1984), after Waldecks Bore. The type section was the interval 577-472m in Barbwire 1; here extended to 577-457m to include Lehmann's overlying informal "upper carbonate member'. Maximum thickness 195m; average c.115m. Mostly indistinguishable from Sahara Formation: mudstone redbed units with evaporites. Deposited under marginal marine to supratidal evaporitic mud flat environments, probably with local eolian influences. Biostratigraphic data detailed.||Worral Formation.||Conformably overlies Elsa Sandstone Member. Is overlain by Tandalgoo Formation, probably unconformably or disconformably.|Mainly red-brown to grey mudstone, often variably calcareous or dolomitic, with interbeds of dolomite, limestone and fine-grained sandstone and dolomite; minor anhydrite common; local significant sandstone sub-units.|
19225|Waldecks Member|69182|6|Mentioned|Ch4 p45|||Canning Basin. Excellent potential seal unit for the storage of carbon dioxide.||Worral Formation|||Shales.|
19230|Walgidee Hills lamproite|41158|6|Mentioned|Fig.130|||See also P162||||||
19251|Wallabi Limestone|23816|6|Mentioned|p256|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
19251|Wallabi Limestone|36890|5|Briefly described|p256|||||||||
19334|Walsh Tillite|22901|6|Mentioned|76 fig 2|||||||||
19334|Walsh Tillite|23557|5|Briefly described|p94|Neoproterozoic|Neoproterozoic|||||||
19334|Walsh Tillite|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Mount House Formation.||||||
19334|Walsh Tillite|24115|5|Briefly described|p32|||Geological Province: Kimberely Basin.||||||
19334|Walsh Tillite|30525|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19334|Walsh Tillite|30533|4|Described|Table 5|||Part of Mount House Group.||||||14-APR-08
19334|Walsh Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19334|Walsh Tillite|30896|4|Described|p18|||||||||
19334|Walsh Tillite|31226|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
19334|Walsh Tillite|32660|5|Briefly described|Table 6|||||||||
19334|Walsh Tillite|32728|6|Mentioned|Fig.16|||See also Table 7||||||
19334|Walsh Tillite|32777|6|Mentioned|p5|||||||||
19334|Walsh Tillite|34287|6|Mentioned|p39|||See also P41||||||
19334|Walsh Tillite|34462|4|Described|Table 1|||Adelaidean||||||
19334|Walsh Tillite|34463|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19334|Walsh Tillite|36048|6|Mentioned|p379|||||||||
19334|Walsh Tillite|36888|4|Described|p213|||||||||
19334|Walsh Tillite|36898|6|Mentioned|p181|||See also P191.||||||
19334|Walsh Tillite|37462|6|Mentioned|p293|||||||||
19334|Walsh Tillite|37927|4|Described|p504|||||||||
19334|Walsh Tillite|38157|6|Mentioned|Table X|||||||||
19334|Walsh Tillite|38243|6|Mentioned|p357|||See also Fig.2.||||||
19334|Walsh Tillite|38988|6|Mentioned|Fig.4|||||||||
19334|Walsh Tillite|39210|5|Briefly described|Fig.18|||||||||
19334|Walsh Tillite|39796|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
19334|Walsh Tillite|41405|5|Briefly described|p206|||||||||
19334|Walsh Tillite|41429|6|Mentioned|p247|||||||||
19334|Walsh Tillite|41453|6|Mentioned|p244|||||||||
19334|Walsh Tillite|42149|6|Mentioned|Table 1 P709|||||||||
19334|Walsh Tillite|42710|5|Briefly described|map legend|Proterozoic||||||||
19334|Walsh Tillite|42811|5|Briefly described|p30|||Of Mount House Group.||||||14-APR-08
19334|Walsh Tillite|43652|6|Mentioned|p385||Neoproterozoic|||||||
19334|Walsh Tillite|44140|5|Briefly described|p300, p301 fig 4-7, p303 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of Mount House area. 10-70m thick. Correlated with Marinoan glaciation (670 Ma).||Mount House Group||Probably equivalent to Moonlight Valley Tillite and Egan Formation.  Overlain conformably by Traine Formation.|Tillite, sandstone and shale; capped by pink dolomite.|08-MAR-18
19334|Walsh Tillite|44363|6|Mentioned|p.15|||||||||
19334|Walsh Tillite|44366|14|Not recorded|p.17, Table 2||Adelaidean|Part of Mt. House Group. Definition on Tech.File E/52-5.||||||
19334|Walsh Tillite|44367|14|Not recorded|map legend||Adelaidean|(Reprinted 1971).||||||
19334|Walsh Tillite|44998|14|Not recorded|p17|||||||||
19334|Walsh Tillite|45923|14|Not recorded|p.72|||||||||
19334|Walsh Tillite|48927|5|Briefly described|p40|||Strat. equiv. See also p39.||||||30-AUG-18
19334|Walsh Tillite|48931|4|Described|p60|||||||||
19334|Walsh Tillite|61571|5|Briefly described|p657|Neoproterozoic|Neoproterozoic|Basal unit of Mount House Gp. Remnants of glacial sediments - contains transported impactites from Spider impact structure. Correlated with Marinoan glaciation (ca610Ma) but palaeomagnetic evidence suggests an older Sturtian glaciation (ca770-750Ma).||||||21-DEC-06
19334|Walsh Tillite|63458|5|Briefly described|p871-881, p891-901.|Cryogenian|Cryogenian|The 'cap dolomicrite' unit is dealt with in detail. Overlies striated pavement.||Unit in Mount House Group.||A correlative of Landrigan and Moonlight Valley Tillites.|Uppermost 4 m comprises a pink-cream, thinly laminated dolomicrite. The underlying deposit of massive diamictite, stratified conglomerate and laminated siltstone varies laterally from tens to hundreds of metres thick.|
19334|Walsh Tillite|63762|5|Briefly described|p19|||See also Walsh Formation.||||||07-FEB-11
19334|Walsh Tillite|64104|6|Mentioned|p63|||The author proposes this name be replaced by Walsh Formation "to distinguish stratigraphic terms from genetic interpretation".||||||
19334|Walsh Tillite|67563|6|Mentioned|p120 Fig.1|||||||||
19334|Walsh Tillite|68244|4|Described|p659-660,671|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. [Potentially referring specifically to glaciogenic tillitic units within the Walsh Formation? Or alternate nomenclature to Walsh Formation].||||||
19334|Walsh Tillite|68277|6|Mentioned|p95, 103|Neoproterozoic|Neoproterozoic|W Kimberley region. Is variously correlated with either the Sturtian or Marinoan glacial level across Australia.|||||Contains a cap carbonate.|
19334|Walsh Tillite|68473|6|Mentioned|p531, p533|||||Duerdin Group||||
19334|Walsh Tillite|69003|6|Mentioned|p48 Fig.57|||Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.||||||
19334|Walsh Tillite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran|Ediacaran|Mount House Sub-basin, Louisa Basin.||Mount House Group|Includes Beverley Springs Member.||matrix-supported, polymictic, pebble-cobble-boulder tillite; matrix is a green siltstone or shale; topped by an algal or stromatolitic dolomite|
19334|Walsh Tillite|69634|4|Described|GEOL_LUT_CSV files|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 Mount House Group.|Includes Beverley Springs Member.||Matrix-supported, polymictic pebble to boulder tillite, green siltstone and shale matrix; capped by microbial to stromatolitic dolomite|
19334|Walsh Tillite|69660|5|Briefly described|Map legend|Cryogenian|Cryogenian|Louisa Basin, North Australian Craton.||Unit in Mount House Group.|Includes Beverley Springs Member.||Matrix-supported, polymictic pebble to boulder tillite, green siltstone and shale matrix; capped by microbial to stromatolitic dolomite.|
19334|Walsh Tillite|70154|4|Described|250k_geologyp_lut.csv|Cryogenian|Cryogenian|See also 250k_interpgeop_lut.csv.|635-850 Ma|Mount House Group|Includes Beverley Springs Member||Matrix-supported, polymictic pebble to boulder tillite, green siltstone and shale matrix; capped by microbial to stromatolitic dolomite|
19334|Walsh Tillite|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 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|720-635 Ma|Unit of Mount House Group.|Includes Beverley Springs Member.||Diamictite with striated pebbles cobbles, boulders of quartzite and lesser siltstone, dolomite and igneous rocks in a green sandy or purple silty matrix, overlain by thinly laminated dolomite; local stromatolitic dolomite and pebbly quartz sandstone|
19334|Walsh Tillite|71288|6|Mentioned|p136|Neoproterozoic|Neoproterozoic|Paleopole positions discussed.||||||
19334|Walsh Tillite|71811|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Louisa Basin.||Mount House Group.||Unconformably overlies Warton Sandstone and Carson Volcanics.|Matrix-supported, polymictic pebble to boulder conglomerate with green siltstone and shale matrix; capped by microbial to stromatolitic dolomite.|
19339|Waltha Woora Formation|22816|6|Mentioned|p15 Fig.7|||||||||
19339|Waltha Woora Formation|23594|4|Described|p22|Neoproterozoic|Neoproterozoic|Of Bangemall Group. Overlain by Paterson Formation. Underlain by Pinjian Chert Breccia. Max. thickness: >300 m.||||||24-JUL-07
19339|Waltha Woora Formation|23745|5|Briefly described|p17|||||||||
19339|Waltha Woora Formation|23746|4|Described|p26|Neoproterozoic|Mesoproterozoic|Of Tarcunyah Group.||||||
19339|Waltha Woora Formation|24025|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin.||||||
19339|Waltha Woora Formation|31308|6|Mentioned|p73|||||||||
19339|Waltha Woora Formation|37460|5|Briefly described|p173|||See also P122||||||
19339|Waltha Woora Formation|37707|6|Mentioned|Fig.2|||See also Table I.||||||
19339|Waltha Woora Formation|38243|6|Mentioned|Fig.2|||||||||
19339|Waltha Woora Formation|38988|6|Mentioned|p6|||||||||
19339|Waltha Woora Formation|39424|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
19339|Waltha Woora Formation|39426|4|Described|p13|||||||||
19339|Waltha Woora Formation|39697|4|Described|p127|||See also p172||||||24-JUL-07
19339|Waltha Woora Formation|41669|6|Mentioned|p46|||||||||
19339|Waltha Woora Formation|42352|6|Mentioned|p5|||Formerly Waltha Woora Beds. Equivalent to Googhenama Formation of the Yeneena Group.||||||
19339|Waltha Woora Formation|43055|6|Mentioned|p28|||||||||
19339|Waltha Woora Formation|44111|6|Mentioned|p.56 Fig.1, p58 Fig. 2, p61 Fig.3|||of Tarcunyah Group. Includes evaporites, stromatolitic carbonates and red beds.||||||
19339|Waltha Woora Formation|44139|6|Mentioned|p279|||An isolated group of dolomite and shale units in the Woodie Woodie area. Includes stromatolites similar to those found in Waroongunyah and Isdell Formations, c.70km to the S.|| ||||06-MAR-18
19339|Waltha Woora Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
19339|Waltha Woora Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
19339|Waltha Woora Formation|45923|14|Not recorded|p.69|||||||||
19339|Waltha Woora Formation|46319|5|Briefly described|p5, p33 App. 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Pilbara Craton.||||||
19339|Waltha Woora Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
19339|Waltha Woora Formation|62453|3|Fully described|p65|||Of the Tarcunyah Group. Geological Province: Paterson Orogen. Overlies Mount Bruce Supergroup. Underlies Paterson Formation. Sandstone, conglomerate, dolomite, shale, siltstone.||||||24-JUL-07
19339|Waltha Woora Formation|63139|5|Briefly described|p50|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Comprises sandstone, conglomerate and carbonate; some manganese has been remobilised into the unit's basal sandstones.||||||07-FEB-08
19339|Waltha Woora Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological Province: Officer Basin (Centralia Superbasin). Stromatolitic dolostone, siltstone, shale, minor sandstone; discontinuous basal sandstone and conglomerate.||||||
19339|Waltha Woora Formation|65366|5|Briefly described|p24|||Northeastern Officer Basin. Includes the Acaciella australica Stromatolite Assemblage||||||
19339|Waltha Woora Formation|65829|5|Briefly described|p27.|||Mixed siliciclastic sedimentary successions that dip off the Pinjian Chert Breccia were included in this unit (Hickman 1978). Subsequent re-mapping showed that it was a westward extension of the Tarcunyah Group (Williams and Trendall 1998a).||Unit in Bangemall Supergroup.||||
19339|Waltha Woora Formation|67183|4|Described|p641,647,650,658,661,664,665,668,671 |Neoproterozoic|Mesoproterozoic|Mn alteration observed within this formation (e.g. Lucy Mack deposit). Previously assigned to the Tarcunyah Group by Williams and Trendall (1998) and Grey et al. (2005), but observations at Woodie Woodie support assigning to the Manganese Subgroup as suggested by Hickman (1978). Its carbonate and sandstone facies are misleadingly capitalised in Tb.1.||Manganese Subgroup||Suggested correlative of the Stag Arrow Formation and Balfour Formation.|Sandstone. At Woodie Woodie - cross-bedded, well-sorted, quartz-rich sandstones and interbedded conglomerate that grades to shale, fine-grained sandstone and dolomitic shale, basal conglomerate with Mn clasts.|
19339|Waltha Woora Formation|67202|5|Briefly described|p52, p66|Neoproterozoic|Neoproterozoic|Deposited in palaeochannels scoured into underlying units. 250-300m thick.||||Unconformably overlies Pinjian Chert Breccia, Carawine Dolomite and Fortescue Group. Is overlain unconformably by Paterson Formation. Proposed correlation with Waroongunyah Formation.|Shale, siltstone, sandstone and dolomitic beds with a locally distributed basal conglomerate.|
19339|Waltha Woora Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Tarcunyah Group|||Stromatolitic dolomite, siltstone, shale, minor sandstone; discontinuous basal sandstone and conglomerate. Sandstone; medium to coarse grained; local pebbly sandstone and conglomerate.|
19339|Waltha Woora 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.|||Stromatolitic dolomite, siltstone, shale, minor sandstone; discontinuous basal sandstone and conglomerate|
19339|Waltha Woora Formation|71042|4|Described|p68-p69|||Officer Basin. On the basis of lithological features and tectonic structures the author has reassigned this unit from the Neoproterozoic Tarcunyah Group to the Mesoproterozoic  Manganese Group.||Manganese Group||Equivalent to the Stag Arrow and Balfour Formations.|Shale, fine-grained sandstone and dolomitic shale and breccia.|24-MAY-19
19339|Waltha Woora Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Stromatolitic dolomite, siltstone, shale, minor sandstone; discontinuous basal sandstone and conglomerate.|
19355|Wandagee Formation|13615|5|Briefly described|p17, p41, p62|Early Permian|Early Permian|Peedamullah Shelf. Also referred to as the Wandagee Limestone on p17, 62. Replaced by Cody Limestone in Ruby 1, Abdul's Dam 1.||of Byro Group.||||11-FEB-19
19355|Wandagee Formation|14228|6|Mentioned|p8|Permian|Permian|||Byro Group||||
19355|Wandagee Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
19355|Wandagee Formation|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
19355|Wandagee Formation|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
19355|Wandagee Formation|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
19355|Wandagee Formation|23726|5|Briefly described|p60|Early Permian|Early Permian|Of Byro Group. Overlying unit Nalbia Sandstone. Underlying unit Quinnanie Shale. Geological Province: Carnarvon Basin.||||||
19355|Wandagee Formation|23815|4|Described|p287|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Minilya Subgroup. Overlying unit: Nalbia Greywacke (conformable). Underlying units: Quinnanie Shale and Cundlego Formation (conformable). Max. thickness: 244 m. Richly fossiliferous.||||||
19355|Wandagee Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
19355|Wandagee Formation|29548|6|Mentioned|p225|||Permian crinoids||||||
19355|Wandagee Formation|30449|6|Mentioned|p11|||Brachiopods. [Originally entered for Qld. CEBMar95]||||||
19355|Wandagee Formation|30545|6|Mentioned|Fig.2|||Part of Byro Group.||||||
19355|Wandagee Formation|32648|6|Mentioned|p32|||in Byro Gp.||||||
19355|Wandagee Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
19355|Wandagee Formation|33710|6|Mentioned|p120|||||||||
19355|Wandagee Formation|33711|6|Mentioned|p384|||||||||
19355|Wandagee Formation|34277|6|Mentioned|Table 1|||Permian||||||
19355|Wandagee Formation|34532|6|Mentioned|p221|||See also PP223,224,etc. L.Perm.||||||
19355|Wandagee Formation|35282|6|Mentioned|Fig.30|||||||||
19355|Wandagee Formation|35530|6|Mentioned|p14|||Location of Bivalvia fossils.||||||
19355|Wandagee Formation|36020|6|Mentioned|p392|||||||||
19355|Wandagee Formation|36257|6|Mentioned|Table 2.1|||||||||
19355|Wandagee Formation|36387|6|Mentioned|p188|||||||||
19355|Wandagee Formation|36740|6|Mentioned|p1|||||||||
19355|Wandagee Formation|36890|3|Fully described|p287|||||||||
19355|Wandagee Formation|37000|6|Mentioned|p23|||||||||
19355|Wandagee Formation|37294|6|Mentioned|p100|||||||||
19355|Wandagee Formation|37295|6|Mentioned|Table 2|||||||||
19355|Wandagee Formation|37304|6|Mentioned|p55|||||||||
19355|Wandagee Formation|37312|6|Mentioned|p7|||||||||
19355|Wandagee Formation|37549|6|Mentioned|p110|||||||||
19355|Wandagee Formation|39223|6|Mentioned|p238|||||||||
19355|Wandagee Formation|39307|6|Mentioned|p438|||||||||
19355|Wandagee Formation|39316|6|Mentioned|Fig.2|||||||||
19355|Wandagee Formation|39615|6|Mentioned|Fig.3|||||||||
19355|Wandagee Formation|39974|6|Mentioned|p113|||||||||
19355|Wandagee Formation|41044|6|Mentioned|p138|||||||||
19355|Wandagee Formation|41049|6|Mentioned|p39|||||||||
19355|Wandagee Formation|41071|6|Mentioned|p25|||||||||
19355|Wandagee Formation|41100|6|Mentioned|Fig.12|||||||||
19355|Wandagee Formation|41271|3|Fully described|p98|||||||||
19355|Wandagee Formation|41438|6|Mentioned|Fig.11|||||||||
19355|Wandagee Formation|41632|6|Mentioned|p4|||||||||
19355|Wandagee Formation|42017|6|Mentioned|p4|||||||||
19355|Wandagee Formation|42116|5|Briefly described|p43|||See also Fig.17||||||
19355|Wandagee Formation|42392|6|Mentioned|p113|||||||||
19355|Wandagee Formation|42462|5|Briefly described|p63|Early Permian||||||||
19355|Wandagee Formation|42540|6|Mentioned|Table 2 P314|||||||||
19355|Wandagee Formation|42654|6|Mentioned|p13|||||||||
19355|Wandagee Formation|42994|6|Mentioned|p51|||||||||
19355|Wandagee Formation|43015|5|Briefly described|Table 1,p319|||||||||
19355|Wandagee Formation|43050|5|Briefly described|p12|||||||||
19355|Wandagee Formation|43471|14|Not recorded|p239|||Megadesmus, Astartila discussed||||||
19355|Wandagee Formation|43474|14|Not recorded|p26|||||||||
19355|Wandagee Formation|44219|14|Not recorded|p31||Artinskian|||||||
19355|Wandagee Formation|44344|14|Not recorded|p.12,15,18,24||Artinskian|Fm. of Minilya Subgroup (Byro Group). Atinskian. (G50-1). opp.4, map.||||||
19355|Wandagee Formation|44345|14|Not recorded|map legend||Artinskian|Artinskian.||||||
19355|Wandagee Formation|44532|4|Described|p.7,8, map|||(G50-5).||||||
19355|Wandagee Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
19355|Wandagee Formation|44537|14|Not recorded|map legend||Artinskian|||||||
19355|Wandagee Formation|44657|14|Not recorded|p.5,6,9,10,16|||||||||
19355|Wandagee Formation|44994|6|Mentioned|Fig.7|||Correlation Permian.||||||
19355|Wandagee Formation|44998|14|Not recorded|App.4 p286|||||||||
19355|Wandagee Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||01-JUN-06
19355|Wandagee Formation|45016|2|Defined|p165-174||Artinskian|Tb. p.89,124,125,131,136,138,143-145,155,157,159,161-4,177,178,181.||||||
19355|Wandagee Formation|45031|14|Not recorded|p22,63||Permian|||||||
19355|Wandagee Formation|48610|14|Not recorded|Pl.1|||||||||
19355|Wandagee Formation|48831|14|Not recorded|p25|||On many pages. p.8,19,25,38,62,68,70,73.||||||
19355|Wandagee Formation|48848|14|Not recorded|p.45|||On many pages. p.22,24-27,31-33,36,38,41,42,45,47,48,52,55,56,61,65,74,76,77,88,98,102,103.||||||
19355|Wandagee Formation|48858|14|Not recorded|p.5-16|||Intermittent turbulence during deposition, i.e. deltaic. (G50-1/Norton). Pl.1,2.||||||
19355|Wandagee Formation|49644|5|Briefly described|Table|||||||||
19355|Wandagee Formation|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of Byro Group. Overlies Quinnanie Shale. Overlain by Nalbia Sandstone. Geological Province: Southern Carnarvon Basin.||||||
19355|Wandagee Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||
19355|Wandagee Formation|64580|5|Briefly described|map legend|||Of Middle Byro Group. Interbedded black mudstone, siltstone, and fine-grained sandstone.||||||15-DEC-08
19355|Wandagee Formation|64974|6|Mentioned|p147 Fig. 5, p149|Kungurian|Kungurian|Geological Province: Carnarvon Basin.||||||24-JUN-09
19355|Wandagee Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark brown siltstone/sandstone heavily bioturbated.|
19355|Wandagee Formation|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 1.77 W/mK. See also p47, p54, app 2 p5.||Byro Group||Overlies Quinnanie Shale, Cundlego Formation, overlain by Nalbia Sandstone|Siltstone and sandstone; heavily bioturbated.|
19355|Wandagee Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.|||Comprises grey siltstone, lesser very fine grained sandstone, and shale.|
19355|Wandagee Formation|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Cundlego Formation, Quinnanie Shale and Bulgadoo Shale as a single unit.||Of the Byro Group.|||Interbedded black mudstone, siltstone and fine-grained sandstone.|06-MAY-14
19355|Wandagee Formation|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
19355|Wandagee Formation|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Nalbia Sandstone and Baker Formation.||Of Byro Group.|||Intercalated siltstone, shale and sandstone.|11-FEB-19
19355|Wandagee Formation|70795|5|Briefly described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group|||Grey siltstone, lesser very fine grained sandstone, and shale.|
19355|Wandagee Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, siltstone|
19355|Wandagee Formation|72910|4|Described|p10, 14, p18, p23, p33, p38, p41.|Kungurian|Kungurian|Thickness 116-202m. Type section: Minilya River, north of Wandagee Hill, 23d44m30sS, 114d25mE. Said to be Artinskian age p38.||Byro Group||Conformably overlies Cundlego Formation, Quinnanie Shale and conformably underlies Nalbia Sandstone, Coolkilya Sandstone.|Grey siltstone, fine sandstone, shale.|
19365|Wandarry Shale|42260|6|Mentioned|p7|||Reserved and previously published as Wandarry Shale Member||||||
19365|Wandarry Shale|61526|5|Briefly described|p880|||Of the Ashburton Formation. Distal, fine-grained. Geological Province: Ashburton Basin.||||||
19365|Wandarry Shale|72712|6|Mentioned|p34.|Statherian|Orosirian|Of Horwitz (1980). Implied to be a member of the Ashburton Formation. 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|||Includes shales.|
19392|Wangarlu Formation|5952|5|Briefly described|p215 Fig. 5, p222, p223|||Appears as Wangarlu in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
19392|Wangarlu Formation|13194|4|Described|p384 Tb. 4-16|Cretaceous|Cretaceous|Type section: Cliffs at NW end of Wangarlu Bay, Cobourg Peninsula. 11o12'S 132o20'E.||Bathurst Island Group||Overlies Darwin Formation (conformably). Part coeval with Moonkinu Sandstone, Turnstone Formation, Vee Formation, Puffin Formation, Brown Gannet Limestone.|Micaceous mudstone, galuconitic siltstone; minor sandstone and carbonate.|
19392|Wangarlu Formation|23999|5|Briefly described|p8|Cretaceous|Cretaceous|Supersedes Wangarlu Mudstone Member. Conformably overlies Darwin Formation; overlain by Mookinu Sandstone. Thickness: 2000m.||||||07-FEB-11
19392|Wangarlu Formation|24001|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Kaolinitic to montmorillonitic claystone/mudstone.||||||18-DEC-06
19392|Wangarlu Formation|24047|5|Briefly described|p13, p63|Cretaceous|Cretaceous|Of the Bathurst Island Group.  Geological Province: Money Shoal Basin.||||||
19392|Wangarlu Formation|24218|5|Briefly described|p850|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
19392|Wangarlu Formation|24379|5|Briefly described|p17|Cretaceous|Cretaceous|Overlies Echuca Shoals Formation. Geological Province: North West shelf.||||||18-DEC-06
19392|Wangarlu Formation|24569|5|Briefly described|p248 Fig. 3|Santonian|Coniacian|Of the Bathurst Island Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
19392|Wangarlu Formation|41459|6|Mentioned|Fig.2|||||||||
19392|Wangarlu Formation|41532|3|Fully described|p306|||||||||
19392|Wangarlu Formation|41731|6|Mentioned|Fig.3|||||||||
19392|Wangarlu Formation|42056|4|Described|p100|||||||||
19392|Wangarlu Formation|42442|2|Defined|p28|Maastrichtian|Albian|NT and WA.||||||18-DEC-06
19392|Wangarlu Formation|42473|6|Mentioned|p56|||||||||
19392|Wangarlu Formation|43661|6|Mentioned|Fig.3|||||||||
19392|Wangarlu Formation|43699|6|Mentioned|Fig.6,p10||Early Cretaceous|||||||
19392|Wangarlu Formation|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Early Cretaceous|||||||
19392|Wangarlu Formation|49637|5|Briefly described|Fig.3|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Geological Province: Petrel Sub-basin.||||||07-FEB-11
19392|Wangarlu Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Early Cretaceous|Of the Bathurst Island Group. Age: ~104-~65Ma. Geological Province: Petrel Sub-basin and Arafura and Money Shoals Basins.||||||01-MAR-10
19392|Wangarlu Formation|64695|5|Briefly described|p262 Fig.8, p265, p266-269 Figs.11-14|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin. A major vitrinite maturity jump at the base of this unit may have been caused by multiple diatreme intrusions.||||Is overlain by Johnson Formation.||
19392|Wangarlu Formation|69452|4|Described|p36:8, 15, 22|Campanian|Albian|Hughes and Senior (1974); Hughes (1978); redefined in Mory (1988). Money Shoal Basin; also Petrel Sub-basin, Bonaparte Basin, where the rocks are referred to as Wangarlu Formation equivalent. Ofshore; <2000m thick. Inner to distal marine shelf.||Bathurst Island Group.||Conformably overlies Darwin Formation.|Massive claystone with subordinate siltstone and minor sandstone, grading upward into claystone, calcimudstone and marl.|12-JUL-16
19392|Wangarlu Formation|69456|3|Fully described|p40:2; 40:3 Fig.40.4; 40:4, 6-8, 10|Cretaceous|Cretaceous|Mory (1988); formerly Wangarlu Mudstone Member of Hughes and Senior (1974). Western Money Shoal Basin, Bonaparte Basin and their offshore areas. Shallow marine environment. 287m thick, thinning to the S; over 2000m in the Malita Graben (offshore Bonaparte Basin). Marine; much of the shale is probably prodeltaic. Contains a relatively diverse, late Albian ammonite fauna. Local 20-30m deep laterite profile capped by ferricrete.||Bathurst Island Group.||Conformably overlies Darwin Formation. Is overlain conformably by Moonkinu Sandstone.|Micaceous mudstone, claystone; variable amounts of glauconitic siltstone, sandstone, marl and limestone. Pyrite, pyritic nodules, calcareous concretions and carbonaceous material are relatively common.|12-JUL-16
19392|Wangarlu Formation|69653|5|Briefly described|p6, 8, 10, 26-27, 30, 37-38, 41-43, 63|Cretaceous|Cretaceous|Petrel Sub-basin. Offshore marine shelf deposits. Schematic (gamma ray) well sections. Composite well diagram. See also p50-51, 53.||Bathurst Island Group.||Overlies Darwin Formation. Is overlain by Woodbine Group.|Fine- to coarse-grained sandstones, packstone limestone, glauconitic argillaceous siltstone, silty mudstone, massive mudstone. Facies described in detail.|
19392|Wangarlu Formation|69673|6|Mentioned|p204|Cretaceous|Cretaceous|||Bathurst Island Group|||Micaceous mudstone with variable amounts of glauconitic siltstone, sandstone, marl and limestone.|
19392|Wangarlu Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Maastrichtian|Albian|See also Regional geology: Fig.6, p12. Sahul: Fig.2, p3. Regionally-developed sandstones form high-quality reservoirs; commonly sealed by Johnson Formation carbonates. Shales and claystones form a regional seal in Sahul Syncline.||Bathurst Island Group.||Overlies Darwin Formation. Is overlain by Woolaston and Puffin Formations.||12-JUL-16
19392|Wangarlu Formation|73083|6|Mentioned|p17|Cretaceous|Cretaceous|Money Shoal Basin.||||||
19416|Wanna Formation|22814|5|Briefly described|fig2|Devonian|Devonian|||||||
19416|Wanna Formation|24390|5|Briefly described|p11 Fig. 6|Devonian|Devonian|Geological Province: Gunbarrel Basin.||||||
19416|Wanna Formation|41751|6|Mentioned|p8|||||||||
19416|Wanna Formation|42030|5|Briefly described|p750|||||||||
19416|Wanna Formation|50085|5|Briefly described|p11 Fig. 6|Devonian|Devonian|Age: <400Ma.  Geological Province: Officer Basin.||||||
19416|Wanna Formation|50205|5|Briefly described|p59 Fig.1,|Devonian|Devonian|Of Gunbarrel Basin.||||Unconformably overlies Lennis Sandstone.||
19416|Wanna Formation|61023|5|Briefly described|p15 Fig. 8|Devonian|Devonian|Geological Province: Gunbarrel Basin.||||||11-APR-08
19416|Wanna Formation|61272|5|Briefly described|p122 Fig.3|||Overlies the Table Hill Volcanics||||||
19416|Wanna Formation|62453|5|Briefly described|p5 Fig. 3|Devonian|Devonian|Geological Province: Officer Basin.||||||
19416|Wanna Formation|64103|6|Mentioned|p400 Fig. 3||Devonian|Formation is Fm in text. Geological Province: Officer Basin.||||||07-FEB-11
19416|Wanna Formation|64325|5|Briefly described|p82 Fig. 2|Early Carboniferous|Late Devonian|Geological Province:Gunbarrel  Basin.||||||26-AUG-08
19416|Wanna Formation|64580|4|Described|map legend|||Fine-grained, well-sorted quartz sandstone; large-scale cross-bedded; minor claystone.||||||09-DEC-08
19416|Wanna Formation|65102|4|Described|p.366,370,373, 374, Figs.4-41,4-49|Carboniferous|Late Devonian|Officer Basin. 10-140m; conformably overlies Lennis Sandstone; fine to medium grained sandstone with minor claystone interbeds; shallow marine; minor intertidal; type section approx 45km SW of Wanna Lake; fission-track anaysis suggests Devonian-Carboniferous.||||||
19416|Wanna Formation|65363|6|Mentioned|p5 Fig.4. |Devonian|Devonian|||||||
19416|Wanna Formation|65416|5|Briefly described|p137, pp144-145.|Early Carboniferous|Devonian|Officer Basin. Part of Sequence Pz4. Sandstone and claystone betweeen 100 and 465 m in Hussar 1, previously interpreted as Lennis Sandstone and Wanna Formation, are now included in Durba Sandstone.||||Unconformably overlies Table Hill Volcanics.||
19416|Wanna Formation|67195|4|Described|p9 fig 5, p10, p19 tbl 1, p46, 47, App 2|Carboniferous|Devonian|Gunbarrel Basin. Thermal conductivity of 2.6 W/mK||||Unconformably overlies Lennis Sandstone, Table Hill Volcanics. Unconformably overlain by Paterson Formation.|Tan fine grained sandstone, faint cross bedding.|
19416|Wanna Formation|67200|5|Briefly described|app 2 p10||||||||Fine grained sandstone ; occasionally mottled.|
19416|Wanna Formation|69003|6|Mentioned|p60|Ordovician|Ordovician|Officer Basin.||||||
19416|Wanna Formation|69029|6|Mentioned|p329|Devonian|Devonian|Of Officer Basin.||||Overlain unconformably by Paterson Formation.||04-SEP-19
19416|Wanna Formation|69091|5|Briefly described|p37|||Officer Basin. Part of an extensive sandstone succession. Appears to be aeolian at least in part.||||Overlain by Paterson Formation; overlies Table Hill Volcanics.||07-OCT-14
19416|Wanna Formation|69153|6|Mentioned|500k_geologyp08_lut.csv||||||||Fine-grained, well-sorted quartz sandstone; large-scale cross-bedded; minor claystone|
19416|Wanna Formation|69445|6|Mentioned|p30:5, 17|||Officer Basin.||||Overlies Table Hill Volcanics.||12-JUL-16
19416|Wanna Formation|70634|5|Briefly described|500k_geolgyp08_lut.csv||||||||Fine-grained, well-sorted quartz sandstone; large-scale cross-bedded; minor claystone.|
19416|Wanna Formation|70772|6|Mentioned|p11|Ordovician|Ordovician|Officer Basin. Age is a detrital zircon maximum depositional age.|c. 650 Ma (Haines et al, 2013)|||||
19416|Wanna Formation|70793|4|Described|500k_interpgeop14_lut.csv|Silurian|Ordovician|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|485.4-419.2 Ma (inferred)||||White-weathering quartz sandstone, minor siltstone; characteristic large to very large scale cross bedding|
19416|Wanna Formation|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Officer Basin.||||||
19416|Wanna Formation|71146|5|Briefly described|p6|Middle Ordovician|Middle Ordovician|Officer Basin.||||Unconformably overlies the Lennis Sandstone.|Sandstone.|
19416|Wanna Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
19416|Wanna Formation|71268|4|Described|GEOL_LUT_CSV files|Silurian|Ordovician|Of Officer Basin (Phase 2). Events: Gondwana breakup-southern margin (100.5-93.9 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|485.4-419.2 Ma (inferred)||||Fine to very fine, well sorted subangular micaceous neritic or non-marine sandstone; minor claystone|
19416|Wanna Formation|71592|5|Briefly described|Appendix A.|||Officer basin.|538+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||White, medium-grained, moderately sorted and rounded, highly friable feldspathic/lithic sandstone; yellow, medium-grained, poorly sorted, highly friable feldspathic/lithic quartz sandstone.|
19416|Wanna Formation|71618|6|Mentioned|p130|Paleozoic|Paleozoic|Of Officer Basin.||||||
19416|Wanna Formation|71800|6|Mentioned|p27|Middle Ordovician|Middle Ordovician|Officer Basin. See Wanna Sandstone Fig.3 p26.|||||Feldspathic sandstone.|18-FEB-19
19416|Wanna Formation|72034|5|Briefly described|500k_interpgeop16_lut|Silurian|Ordovician|Officer Basin (Phase 2).|||||White-weathering quartz sandstone, minor siltstone; characteristic large to very large scale cross bedding.|
19416|Wanna Formation|73346|6|Mentioned|p25|||Officer Basin. [Written as ?Wanna Formation].||||||
19445|Warburton Porphyry|30390|6|Mentioned|p49|||||||||
19452|Wardens Hill conglomerate|29784|6|Mentioned|p54|||||||||
19470|Warnbro Group|12758|4|Described|p21, p3 Fig. 3|Late Cretaceous|Early Cretaceous|Comprises 3 sub-units: Gage Formation, South Perth Shale and Leederville Formation (Davidson, 1995).  Max. thickness: 1382m.  See also p8 Fig. 9 and p10 Fig. 10. Geological Province: Perth Basin.||||||22-DEC-06
19470|Warnbro Group|12759|5|Briefly described|p34; p28 Tb. 7; p32 Fig 15.|Aptian|Valanginian|Defined Cockbain and Playford (1973).|||Includes Gage and Leederville Formations and South Perth Shale.|Unconformably overlies Cattamarra Coal Measures, Yarragadee or Parmelia Formations.||12-MAY-14
19470|Warnbro Group|14227|5|Briefly described|p8, p12|Barremian|Valanginian|Includes the Gage Sandstone, South Perth Shale and Leederville Formation. Thickness: 1500m. Geological Province: Vlaming Sub-basin. Clastics - with basinal turbidites up through to deltaic and fluvial facies. See also Enclosure 2.||||||07-FEB-11
19470|Warnbro Group|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
19470|Warnbro Group|22820|5|Briefly described|p22-23|Cretaceous|Cretaceous|Includes Leederville Formation and Bunbury Basalt.||||||12-AUG-08
19470|Warnbro Group|23279|4|Described|p30|Aptian|Neocomian|(Cockbain and Playford, 1973).||||||
19470|Warnbro Group|23816|4|Described|p246, 247|||Geological Province: Perth Basin. Contains the South Perth Shale, Leederville Formation and Dandaragan Sandstone. Max. thickness: 1201 m.||||||
19470|Warnbro Group|24160|5|Briefly described|p94|Early Cretaceous|Early Cretaceous|Text specifies "consists of the lower South Perth Shale and the upper Leederville Formation"; [what happens to the rest of these units?].|||South Perth Shale, Leederville Formation.|||
19470|Warnbro Group|24443|5|Briefly described|p23, Fig.30|Early Cretaceous|Early Cretaceous|Unconfromably overlies Yarragadee Formation and Parmelia Group. Unconformably overlain by Coolyena Group.  Geological Province: Vlaming Sub-basin.||||||
19470|Warnbro Group|29382|6|Mentioned|Table 10|||||||||
19470|Warnbro Group|29693|6|Mentioned|Fig.7|||||||||
19470|Warnbro Group|30188|2|Defined|p74|Aptian|Neocomian|Neocomian to Aptian||||||
19470|Warnbro Group|30217|6|Mentioned|p20|||Lower Cretaceous age. Stratigraphy||||||
19470|Warnbro Group|30268|6|Mentioned|p44|||||||||
19470|Warnbro Group|31153|6|Mentioned|Fig. 57|||Refers Cockbain & Playford (1973).||||||
19470|Warnbro Group|31238|4|Described|p27|||||||||
19470|Warnbro Group|34841|6|Mentioned|Fig.2|||||||||
19470|Warnbro Group|35093|6|Mentioned|p22|||||||||
19470|Warnbro Group|35152|6|Mentioned|p3|||||||||
19470|Warnbro Group|35638|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19470|Warnbro Group|35653|6|Mentioned|Fig.3|||Stratigraphy of Dandaragan Trough.||||||
19470|Warnbro Group|35968|6|Mentioned|Table 4|||||||||
19470|Warnbro Group|35970|6|Mentioned|p77|||||||||
19470|Warnbro Group|36100|6|Mentioned|Fig.2|||||||||
19470|Warnbro Group|36265|5|Briefly described|Fig.3.26|Early Cretaceous|Early Cretaceous|Includes the South Perth Shale and Leederville Formation. Geological province: Perth Basin.||||||04-MAR-08
19470|Warnbro Group|36293|2|Defined|p165|Early Cretaceous|Early Cretaceous|||||||
19470|Warnbro Group|36890|4|Described|p246|||||||||
19470|Warnbro Group|37104|6|Mentioned|Fig.3|||||||||
19470|Warnbro Group|39554|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19470|Warnbro Group|40300|6|Mentioned|p1|||||||||
19470|Warnbro Group|40348|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19470|Warnbro Group|40349|4|Described|p16|||||||||
19470|Warnbro Group|40367|5|Briefly described|p72, p81|Early Cretaceous|Early Cretaceous|This group's weathered plain is overlain by calcareous sands and muds of Australind Formation.||||||07-AUG-07
19470|Warnbro Group|40395|6|Mentioned|p332|||||||||
19470|Warnbro Group|40992|6|Mentioned|Fig.5|||||||||
19470|Warnbro Group|41195|6|Mentioned|Fig.2|||||||||
19470|Warnbro Group|41728|6|Mentioned|p441|||||||||
19470|Warnbro Group|41780|5|Briefly described|p3|||||||||
19470|Warnbro Group|41989|6|Mentioned|p112|||||||||
19470|Warnbro Group|42075|5|Briefly described|Fig.7 P247|||||||||
19470|Warnbro Group|42194|6|Mentioned|p5|||||||||
19470|Warnbro Group|42431|6|Mentioned|p237|||Perth Basin||||||
19470|Warnbro Group|42434|4|Described|p5|||||||||
19470|Warnbro Group|43096|5|Briefly described|p6|||||||||
19470|Warnbro Group|43197|5|Briefly described|Map Legend||Cretaceous|||||||
19470|Warnbro Group|43212|5|Briefly described|p6||Early Cretaceous|||||||
19470|Warnbro Group|43347|4|Described|9||Early Cretaceous|||||||
19470|Warnbro Group|44144|4|Described|p504 Tb.4-21, p509 fig 4-145, p516-517|Early Cretaceous|Early Cretaceous|See also p524. Cockbain and Playford (1973).|||Includes South Perth Shale, Leederville Formation and Dandaragan Sandstone.|||
19470|Warnbro Group|50107|5|Briefly described|Map legend|Cretaceous|Cretaceous|Geological Province: Perth Basin.||||||
19470|Warnbro Group|50108|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin.||||||
19470|Warnbro Group|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Includes; Gage Sandstone, South Perth Shale and Leederville Formation. Overlain unconformably by Coolyena Group. Underlain unconformably by Charlotte Sandstone (Parmelia Group).||||||07-FEB-11
19470|Warnbro Group|61811|5|Briefly described|p3 Fig.2, p55 Table 7, p57.|Early Cretaceous|Early Cretaceous|Northern Perth Basin.|||Includes Dandaragan Sandstone, South Perth Shale and Leederville Formation.|Is unconformably overlain by Coolyena Group (Molecap Greensand and Osborne Formation).||
19470|Warnbro Group|64580|4|Described|map legend||Early Cretaceous|Interbedded sandstone, siltstone and shale; minor conglomerate; includes DANDARAGAN SANDSTONE, SOUTH PERTH SHALE and LEEDERVILLE FORMATION.||||||09-DEC-08
19470|Warnbro Group|64635|5|Briefly described|p4 Fig.3 |Hauterivian|Berriasian||||Includes South Perth Shale and Leederville Formation.|||
19470|Warnbro Group|67115|6|Mentioned|p63, p67, p69|Cretaceous|Cretaceous||||Leederville Formation.|||
19470|Warnbro Group|67340|6|Mentioned|p6, 8, 25|Early Cretaceous|Early Cretaceous|Northern Perth Basin. Its base marks the Early Cretaceous breakup unconformity. Thermal rock properties.|||South Perth Shale, Leederville Formation.|||
19470|Warnbro Group|67925|5|Briefly described|Ch2 p10 fig 4, Ch2 p11|Aptian|Valanginian|See also Ch4 p8 fig 2, Ch4 p30 fig 34, Ch8 p11.|||Includes the Leederville Formation.|Unconformably overlies the Parmelia Group and the Willespie Formation. Unconformably overlain by the Coolyena Group.||
19470|Warnbro Group|68254|6|Mentioned|p1037 Tb.2||||||Includes Leederville Formation.|||
19470|Warnbro Group|69081|5|Briefly described|p737 Fig.1|Early Cretaceous|Early Cretaceous|Geol. Prov: Perth Basin.|||Leederville Formation, South Perth Shale, Gage Sst|Is unconformably overlain by Coolyena Group; unconformably overlies Parmelia Group.||23-JUL-15
19470|Warnbro Group|69182|5|Briefly described|Ch2 p3, Ch2 p9|||Perth Basin. See also Ch2 p45-p46, Ch2 p55, Ch2 p57.|||Includes the South Perth Shale, Gage Sandstone and the Leederville Formation.|Unconformably overlies the Parmelia Group and the Bunbury Basalt.  Unconformably overlain by the Coolyena Group.||
19470|Warnbro Group|69297|6|Mentioned|p175, p189|Aptian|Valanginian|Vlaming Sub-basin, South Perth Basin.|||Includes the Gage Sandstone, South Perth Shale and the Leederville Formation.|Overlain by the Coolyena Group.||
19470|Warnbro Group|70097|5|Briefly described|p3, p19 Fig.3, p20 Fig.4|Aptian|Valanginian|Marine sediments deposited after local subsidence. Perth Basin. Dandaragan Trough, Beermullah Trough, Mandurah Terrace, Vlaming Sub-basin and Bunbury Trough.|||Leederville Formation, South Perth Shale, Gage Sandstone, Bunbury Basalt|Overlies Parmelia Group or Yarragadee Formation. Is overlain by Coolyena Group or Yoganup Formation.|Marine sediments (including turbidites) and volcanics.|12-SEP-17
19470|Warnbro Group|70099|5|Briefly described|Fig.4|Aptian|Valanginian|Mentelle 5a, 5b, 6 and 7a Supersequences.|||Gage Sandstone, South Perth Shale, Leederville Formation.|Is overlain by Coolyena Group.||
19470|Warnbro Group|70128|5|Briefly described|p449, p451, p463|Early Cretaceous|Early Cretaceous|Perth Basin.|||Gage Sandstone, South Perth Shale, Leederville Formation.|Unconformably overlies Parmelia Group. Is overlain unconformably by Coolyena Group.||
19470|Warnbro Group|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Perth Basin.||||||
19470|Warnbro Group|71377|5|Briefly described|p7, p9|Early Cretaceous|Early Cretaceous|Perth Basin.|||Includes the South Perth Shale, Bunbury Basalt and the Leederville Formation.|||
19470|Warnbro Group|71958|5|Briefly described|p6, p14-p15, p18, p34-p39|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin, Perth Basin. Dominated by deltaic and shallow marine successions. Several potential plays are described in Miyazaki et al (1996).|||Includes the Gage Sandstone, Leederville Formation and the South Perth Shale.|Unconformably overlies the Charlotte Sandstone, Carnac Formation and Jervoise Sandstone (Parmelia Group). Overlain by the Coolyena Group.||
19470|Warnbro Group|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Valanginian|Perth Basin.  Age from biostratigraphy.|||Includes Leederville Formation.||Interbedded sandstone, siltstone, and shale; minor conglomerate.|
19479|Waronga gneiss|32637|4|Described|p8|||||||||
19479|Waronga gneiss|35113|5|Briefly described|p57|||||||||
19484|Warra Warringa Formation|23815|4|Described|p286|Artinskian|Artinskian|Geological Province: Byro Sub-basin. Uppermost unit of the Newman Subgroup. Underlying unit: Bogadi Greywacke (conformable). Max. thickness: 50 m.||||||27-APR-05
19484|Warra Warringa Formation|32648|6|Mentioned|p32|||in Byro Gp.||||||
19484|Warra Warringa Formation|33594|6|Mentioned|p37|||||||||
19484|Warra Warringa Formation|34532|6|Mentioned|p225|||||||||
19484|Warra Warringa Formation|36890|3|Fully described|p286|||||||||
19484|Warra Warringa Formation|37295|6|Mentioned|p54|||See also Table 2.||||||
19484|Warra Warringa Formation|41053|6|Mentioned|Fig.2|||||||||
19484|Warra Warringa Formation|44994|6|Mentioned|Fig.7|||Correlation||||||
19484|Warra Warringa Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Unit of Newman Sub-Group (Byro Group).||||||01-JUN-06
19484|Warra Warringa Formation|45016|2|Defined|p154||Artinskian|Tb, p.124,125,126,143-5,151. See also Warrawarringa Formation.||||||
19484|Warra Warringa Formation|48885|14|Not recorded|p.2||Early Permian|Lower Permian (Sakmarian-Artinskian).||||||
19484|Warra Warringa Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Newman Sub-Group (Byro Group).||||||21-MAR-06
19485|Warrada Dolomite Member|22905|6|Mentioned|p53|||Of Daniels (1970).  Probably equivalent of the more recent Cheyne Springs Formation (Chuck, 1984).||||||20-MAY-04
19485|Warrada Dolomite Member|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Irregully Formation.||||||
19485|Warrada Dolomite Member|34066|4|Described|p11|||Mid.Prot.||||||
19485|Warrada Dolomite Member|36884|4|Described|p153|||||||||
19485|Warrada Dolomite Member|40089|4|Described|p24|||||||||
19485|Warrada Dolomite Member|44481|5|Briefly described|map legend||Mesoproterozoic|Part of Irregully Formation.||||||
19485|Warrada Dolomite Member|72758|5|Briefly described|p8 Tb.1, p50, p52-53.|||640 m thick.  Part of the 2800m thick Irregully Formation. Not present south of Ashburton River.||Irregully Formation||Conformably overlies the Gooragoora Sandstone Member and conformably underlies the Revels Corner Sandstone Member.|Massive, cream weathering dolomite in lower half; upper half, well-bedded edgewise conglomerate and silicified horizons.|
19492|Warramboo Sandstone|22484|5|Briefly described|p83 Fig13|||of the Mount Minnie Group||||||
19492|Warramboo Sandstone|23325|5|Briefly described|map legend|Proterozoic|Proterozoic|of Mount Minnie Group||||||
19492|Warramboo Sandstone|24544|4|Described|p48|Paleoproterozoic|Paleoproterozoic|Of Mount Minnie Group. Quartz sandstone, minor siltstone and mudstone. Geological Province: Ashburton Province.||||||07-NOV-08
19492|Warramboo Sandstone|34066|4|Described|p9|||See also P10. Mid.Prot.||||||
19492|Warramboo Sandstone|36883|4|Described|p146|||||||||
19492|Warramboo Sandstone|37460|6|Mentioned|p157|||||||||
19492|Warramboo Sandstone|42260|4|Described|p99|||||||||
19492|Warramboo Sandstone|44477|2|Defined|p.29, p.13, Table 1||Proterozoic|SF/50-6.||||||
19492|Warramboo Sandstone|44478|14|Not recorded|map legend||Proterozoic|||||||
19492|Warramboo Sandstone|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
19492|Warramboo Sandstone|67855|5|Briefly described|p221|||400m thick.||Mount Minnie Group||Overlies Wabco Shale (conformably) or Brodagee Sandstone (conformably).|Thin to medium bedded, fine to coarse grained sandstone with minor mudstone.|
19492|Warramboo Sandstone|69028|5|Briefly described|Map Legend|Statherian|Statherian|Ashburton and Blair Basins. Mapped with Wabco Shale and Brodagee Sandstone as a single unit.||Of the Mount Minnie Group.|||Quartz sandstone, conglomerate, siltstone and mudstone.|07-MAY-14
19492|Warramboo Sandstone|72758|5|Briefly described|p10 Tb.1, p48-49.|||About 400 m thick. Braided fluvial to shallow-marine.||Mount Minnie Group||Conformably overlies Wabco Shale. Disconformably overlies Brodagee Sandstone.|Thin-medium bedded, fine to coarse sandstone and minor mudstone; sandstone often cross-stratified, current ripples and small scale slumps.|
19508|Warrawoona Group|22449|6|Mentioned|P25, Fig27 P26||Archean|Age of unit is >3430 Ma||||||07-NOV-08
19508|Warrawoona Group|22615|4|Described|p 2||Archean|North Pole Dome.   Age 3460Ma.||||||07-NOV-08
19508|Warrawoona Group|22642|6|Mentioned|485|||Geol province Pilbara Craton. Overlying unit Gorge Creek Group||||||
19508|Warrawoona Group|22672|6|Mentioned|P268|||||||||
19508|Warrawoona Group|22715|5|Briefly described|fig7,table7,p214,216|Archean|Archean|||||||07-NOV-08
19508|Warrawoona Group|22717|5|Briefly described|P4, Fig3 P18||Archean|||||||07-NOV-08
19508|Warrawoona Group|22727|6|Mentioned|p635,8||Archean|||||||07-NOV-08
19508|Warrawoona Group|22899|5|Briefly described|85|||||||||
19508|Warrawoona Group|23033|5|Briefly described|156|||||||||
19508|Warrawoona Group|23128|5|Briefly described|p372|||||||||
19508|Warrawoona Group|23206|6|Mentioned|p1256-1262 Fig.1||Archean|Age: 3.47 - 3.43 Ga. of Pilbara Supergroup.||||||07-NOV-08
19508|Warrawoona Group|23244|6|Mentioned|p15|||of Pilbara Supergroup.||||||
19508|Warrawoona Group|23255|6|Mentioned|p46 Fig.2||Archean|Deposition between 3487 and 3430 Ma.||||||07-NOV-08
19508|Warrawoona Group|23388|6|Mentioned|p14 Table 1|||||||||
19508|Warrawoona Group|23415|6|Mentioned|Map Legend (Simplified geol.)|||Geological province: Pilbara Craton.||||||07-JAN-08
19508|Warrawoona Group|23416|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup, Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|23484|5|Briefly described|p5|Archean|Archean|Age: 3500-3400Ma.||||||07-NOV-08
19508|Warrawoona Group|23570|5|Briefly described|p11|||Geological Province: Pilbara Craton||||||
19508|Warrawoona Group|23585|5|Briefly described|p10 Table 1|Archean|Archean|||||||07-NOV-08
19508|Warrawoona Group|23598|5|Briefly described|p3|||Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||
19508|Warrawoona Group|23743|6|Mentioned|p3|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|23755|4|Described|p19|Archean|Archean|See also page 17 table 1.||||||07-NOV-08
19508|Warrawoona Group|23757|4|Described|p8|Archean|Archean|Age: <3048 Ma (SHRIMP U-Pb zircon). Geological Province: Pilbara Craton - in theYarrie greenstone belt, but postulated to continue N-NE into COORAGOORA under cover of Gorge Creek and De Grey Groups, and Eel Creek and Callawa Formations..||||||07-NOV-08
19508|Warrawoona Group|23780|5|Briefly described|p111|Archean|Archean|Age: ~3433-3451 Ma.||||||07-NOV-08
19508|Warrawoona Group|23783|4|Described|p11|Archean|Archean|Of the Pilbara Supergroup.||||||07-NOV-08
19508|Warrawoona Group|23784|5|Briefly described|p2|Archean|Archean|Age: 3480-3410Ma.||||||07-NOV-08
19508|Warrawoona Group|23789|6|Mentioned|p35|||Geological Province: Pilbara Craton.||||||
19508|Warrawoona Group|23793|4|Described|p9|||Of Pilbara Supergroup||||||
19508|Warrawoona Group|23807|5|Briefly described|p109|||Geological Province: Pilbara Craton.||||||
19508|Warrawoona Group|23813|5|Briefly described|p101|Archean|Archean|Tholeiites, high-Mg basalts, andesite, Na-dacite, K-rhyolites, chert, minor banded iron formation.  Age: c.2.48-2.43Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
19508|Warrawoona Group|23891|5|Briefly described|p89|Archean|Archean|Of Mount Bruce Supsergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|23895|5|Briefly described|p884 Fig.1|||Geological Province: Pilbara Craton.  Geological Province: Pilbara Craton.||||||07-MAR-05
19508|Warrawoona Group|23936|4|Described|p2|Archean|Archean|Age: ca. 3490-3410 Ma. Geological Province: Pilbara Craton. Underlain by Coonterunah Group. Overlain by Wyman Formation (unconformably) & Sulphur Springs Group (unconformably).||||||07-NOV-08
19508|Warrawoona Group|23956|4|Described|p1264|Archean|Archean|Age: ca. 3.46 Ga. Unconformably overlain by the Sulphur Springs Group. Overlies the Coonterunah Group. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|23980|14|Not recorded|p291|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24016|5|Briefly described|p293 (in title only)|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24025|4|Described|p9 Tb. 1|Archean|Archean|Contains the Salgash and Talga Talga Subgroups.  Age: c.3480-3340Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24095|4|Described|p46|||Basal unit of the Pilbara Supergroup. Overlain by Gorge Creek Group. Geological Province: Pilbara Block.||||||14-APR-08
19508|Warrawoona Group|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Pilbara Supergroup.   Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24166|5|Briefly described|p9|Archean|Archean|Parent: Pilbara Supergroup.   Age: c.3460Ma.   Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24169|5|Briefly described|p666 Fig. 5|Archean|Archean|Geological Province : Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24182|4|Described|p92|Archean|Archean|Max Thickness: 10km.  Geological Province: Pilbara Craton. Age: 3490 - 3426 Ma. Of the Warrawoona Megasequence of Krapez, 1993.||||||07-NOV-08
19508|Warrawoona Group|24184|4|Described|p699|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton. Age: ca.3.49-3.31Ga. Now includes the newly defined Kelly Subgroup (Bagas and Kranendonk, unpub. data) together with the Talga Talga and Salgash Subgroups.||||||07-NOV-08
19508|Warrawoona Group|24186|4|Described|p776, 777 Fig.2|Archean|Archean|Age: ca. 3460Ma (Hickman, 1983; Neumayr, 1993). Underlying Unit: Coonterunah Group. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24187|5|Briefly described|p776, 777 Fig.2|Archean|Archean|Age: ca. 3460 Ma (Hickman, 1983; Neumayr, 1993). Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24188|4|Described|p789, 795|Archean|Archean|Age: ca. 3475-3450 Ma (Hickman, 1983). Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24194|6|Mentioned|p908|||||||||
19508|Warrawoona Group|24327|5|Briefly described|Map Legend|Archean|Archean|Parent: Pilbara Supergroup.  Includes the Euro Basalt.  Age: <3475Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24349|5|Briefly described|Map legend|Archean|Archean|Of Pilbara Supergroup.   Age: <3475Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|24531|5|Briefly described|p11, p5|Archean|Archean|Of the Pilbara Supergroup.  Unconformably overlies the Coonterunah Group. Conformably overlain by the Leilira Formation.  Age: c.3490-3319Ma.  Geological Province: Pilbara Craton.  See also p5 Table 1.||||||07-NOV-08
19508|Warrawoona Group|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: c.3434Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24541|5|Briefly described|p7|Archean|Archean|Age: c. 3500-3400 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|24550|5|Briefly described|p30, p31 Tb. 3.1|Archean|Archean|Subdivided into: Talga Talga, Salgash + Kelly Subgroups. Consists of clastic seds, pillow basalts + minor komatiites. Unconformably overlies Coonterunah Group; unconformably overlain by Gorge Creek Group. Age: ca 3475-3435Ma. Geol Prov: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|24590|5|Briefly described|p16, p30 Fig. 1.3|Archean|Archean|Includes the Salgash and Talga Talga Subgroups. Age: 3560+/-32-<3417+/-9Ma. See also p28 Fig. 1.2.||||||07-FEB-11
19508|Warrawoona Group|24621|4|Described|p80|Archean|Archean|Unconformably overlain by the Gorge Creek Group; overlies Coonterunah Group unconformably and the Carlindi granodiorite. Age: ~3.46 Ga. Max. thickness: 4km.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|30484|6|Mentioned|p58|||Refs Hickman 1975||||||
19508|Warrawoona Group|30485|6|Mentioned|p74|||Refers Lipple 1975||||||
19508|Warrawoona Group|31308|6|Mentioned|p65|||Precambrian Stratigraphy||||||
19508|Warrawoona Group|31310|6|Mentioned|p55|||||||||
19508|Warrawoona Group|31819|6|Mentioned|p80|||||||||
19508|Warrawoona Group|31853|2|Defined|p60|Archean|Archean|||||||07-NOV-08
19508|Warrawoona Group|34731|6|Mentioned|p808|||||||||
19508|Warrawoona Group|34829|6|Mentioned|p67|||||||||
19508|Warrawoona Group|35142|6|Mentioned|p421|||See also Fig.1||||||
19508|Warrawoona Group|35218|6|Mentioned|p1|||||||||
19508|Warrawoona Group|35531|4|Described|p74|||Sedimentological aspects discussed||||||
19508|Warrawoona Group|35681|6|Mentioned|p10|||||||||
19508|Warrawoona Group|35726|6|Mentioned|p120|||||||||
19508|Warrawoona Group|35949|6|Mentioned|p333|||||||||
19508|Warrawoona Group|36123|6|Mentioned|p443|||||||||
19508|Warrawoona Group|36124|5|Briefly described|p441|||||||||
19508|Warrawoona Group|36125|6|Mentioned|p396|||||||||
19508|Warrawoona Group|36257|6|Mentioned|Fig.2.1|||||||||
19508|Warrawoona Group|36551|6|Mentioned|p55|||||||||
19508|Warrawoona Group|36744|6|Mentioned|p53|||||||||
19508|Warrawoona Group|37269|6|Mentioned|p161|||||||||
19508|Warrawoona Group|37299|6|Mentioned|Fig.1|||||||||
19508|Warrawoona Group|37577|6|Mentioned|p26|||||||||
19508|Warrawoona Group|37633|4|Described|p12|||See also Plate 1 and P51.||||||
19508|Warrawoona Group|37899|6|Mentioned|Fig.2|||||||||
19508|Warrawoona Group|38242|5|Briefly described|p200|||See also P199.||||||
19508|Warrawoona Group|38258|5|Briefly described|p1231|||||||||
19508|Warrawoona Group|38300|6|Mentioned|p401|||||||||
19508|Warrawoona Group|38461|5|Briefly described|p1581|||||||||
19508|Warrawoona Group|38481|4|Described|p265|||||||||
19508|Warrawoona Group|38498|4|Described|p62|||See also Fig.1 and P58.||||||
19508|Warrawoona Group|38507|5|Briefly described|p236|||||||||
19508|Warrawoona Group|38508|4|Described|p225|||||||||
19508|Warrawoona Group|38510|6|Mentioned|Table 1|||||||||
19508|Warrawoona Group|38542|6|Mentioned|p361|||||||||
19508|Warrawoona Group|38544|6|Mentioned|p289|||||||||
19508|Warrawoona Group|38624|4|Described|p240|||||||||
19508|Warrawoona Group|38742|5|Briefly described|p354|||||||||
19508|Warrawoona Group|38767|5|Briefly described|p91|||||||||
19508|Warrawoona Group|38946|4|Described|p361|||||||||
19508|Warrawoona Group|39310|6|Mentioned|p26|||||||||
19508|Warrawoona Group|39328|6|Mentioned|p475|||||||||
19508|Warrawoona Group|39426|6|Mentioned|p4|||||||||
19508|Warrawoona Group|39444|6|Mentioned|p6|||||||||
19508|Warrawoona Group|39477|6|Mentioned|p327|||||||||
19508|Warrawoona Group|39580|4|Described|p288|||||||||
19508|Warrawoona Group|39634|6|Mentioned|p169|||||||||
19508|Warrawoona Group|39672|5|Briefly described|Fig.2|||||||||
19508|Warrawoona Group|39697|3|Fully described|p87|||||||||
19508|Warrawoona Group|40183|6|Mentioned|p309|||||||||
19508|Warrawoona Group|40596|6|Mentioned|p65|||||||||
19508|Warrawoona Group|40661|5|Briefly described|p90|||||||||
19508|Warrawoona Group|40899|6|Mentioned|Fig.1|||||||||
19508|Warrawoona Group|41028|5|Briefly described|p227|||||||||
19508|Warrawoona Group|41073|5|Briefly described|p200|||||||||
19508|Warrawoona Group|41096|5|Briefly described|p305|||||||||
19508|Warrawoona Group|41250|5|Briefly described|p31|||See also P29||||||
19508|Warrawoona Group|41252|5|Briefly described|p49|||||||||
19508|Warrawoona Group|41263|6|Mentioned|p57|||||||||
19508|Warrawoona Group|41349|6|Mentioned|p2|||||||||
19508|Warrawoona Group|41350|5|Briefly described|p23|||||||||
19508|Warrawoona Group|41351|5|Briefly described|p37|||||||||
19508|Warrawoona Group|41352|6|Mentioned|p54|||||||||
19508|Warrawoona Group|41353|6|Mentioned|p69|||||||||
19508|Warrawoona Group|41354|5|Briefly described|p90|||||||||
19508|Warrawoona Group|41355|6|Mentioned|Fig.2|||||||||
19508|Warrawoona Group|41357|6|Mentioned|Fig.1|||||||||
19508|Warrawoona Group|41358|6|Mentioned|Fig.1|||||||||
19508|Warrawoona Group|41561|5|Briefly described|p535|||||||||
19508|Warrawoona Group|41594|6|Mentioned|p70|||||||||
19508|Warrawoona Group|41624|5|Briefly described|p43|||||||||
19508|Warrawoona Group|41635|5|Briefly described|p21|||||||||
19508|Warrawoona Group|41636|6|Mentioned|p79|||||||||
19508|Warrawoona Group|41678|6|Mentioned|p30|||||||||
19508|Warrawoona Group|41767|4|Described|p44|||||||||
19508|Warrawoona Group|41851|5|Briefly described|p822|||||||||
19508|Warrawoona Group|41892|6|Mentioned|p315|||||||||
19508|Warrawoona Group|41938|5|Briefly described|p9|||||||||
19508|Warrawoona Group|41956|4|Described|p248|||||||||
19508|Warrawoona Group|41982|6|Mentioned|Table 1 P1780|||||||||
19508|Warrawoona Group|42231|4|Described|p330|||||||||
19508|Warrawoona Group|42329|5|Briefly described|p3|||||||||
19508|Warrawoona Group|42342|5|Briefly described|p20|||3500-3300 Myr||||||
19508|Warrawoona Group|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
19508|Warrawoona Group|42730|4|Described|p4|||||||||
19508|Warrawoona Group|42973|5|Briefly described|p175|||||||||
19508|Warrawoona Group|43052|5|Briefly described|Fig.3.8|||||||||
19508|Warrawoona Group|43057|6|Mentioned|p54|||||||||
19508|Warrawoona Group|43562|4|Described|p574|||Age: 3.46 GYr.||||||14-APR-08
19508|Warrawoona Group|43595|4|Described|p213|||||||||
19508|Warrawoona Group|43644|6|Mentioned|Fig.4,p591|||||||||
19508|Warrawoona Group|43673|6|Mentioned|p374|||Ejecta age: approx. 3.45 Ga||||||
19508|Warrawoona Group|43689|6|Mentioned|Fig3p166|||||||||
19508|Warrawoona Group|43698|6|Mentioned|p3||Archean|Late Archaean||||||07-NOV-08
19508|Warrawoona Group|43769|6|Mentioned|p855|||Age: 3.46 Ga||||||
19508|Warrawoona Group|43779|5|Briefly described|p1-21||Archean|||||||07-NOV-08
19508|Warrawoona Group|44150|4|Described|p128, p129 Tb.2-15, p132 Figs.2-131,-132|||See also p134-137, p139-142, p152. Total thickness 15km.|3.6-3.3 Ga.|Pilbara Supergroup|Talga Talga, Salgash Subgroups; Duffer, Wyman Formations.|Intruded by Woodstock and Mondana Adamellites.|Basalt and chert Subgroups separated by felsic-Volcanics.|
19508|Warrawoona Group|44229|5|Briefly described|Map Legend|Archean|Archean|Subdivided into the Salgash and Talga Talga Subgroups.||||||07-NOV-08
19508|Warrawoona Group|46319|5|Briefly described|p3|Archean|Archean|Of Pilbara Supergroup.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|46922|6|Mentioned|p259|||Trace element analysis.||||||
19508|Warrawoona Group|50287|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|50379|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|50381|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|50383|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton||||||07-NOV-08
19508|Warrawoona Group|50423|4|Described|p215 Fig.1, p216||Archean|Unconformably overlies Coonterunah Group. Contains no internal unconformities. Here informally divided into upper and lower sections.  East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
19508|Warrawoona Group|50427|4|Described|p182 Fig.5|Archean|Archean|Age: 3490-3320 Ma. Overlies Coonterunah Group and locally younger granitoid rocks. Overlain unconformably by Budjan Creek Formation, De Grey Group, and conformably by Golden Cockatoo Formation and Wyman Formation. Of Pilbara Supergroup.||||||07-NOV-08
19508|Warrawoona Group|50430|4|Described|p154||Archean|Age: 3320-3480 Ma. Predominantly volcanic deposits on basement of earlier granite-greenstones. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
19508|Warrawoona Group|50435|6|Mentioned|p2.1|||Intruded by Bridget Suite.  Geological Province: Kimberley Block.||||||
19508|Warrawoona Group|50542|6|Mentioned|p25,|Archean|Archean|||||||07-FEB-11
19508|Warrawoona Group|50544|3|Fully described|p18, p69|Archean|Archean|Of the Pilbara Supergroup. Subdivided into: Talga Talga and Salgash Subgroups, separated by Duffer Formation; now proposed that Kelly Subgroup should become third subgroup.  Age: c.3490-3310Ma (Williams, 1999a; Van Kranendonk et al, 2001).||||||23-DEC-09
19508|Warrawoona Group|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Kelly, Salgash and Talga Talga Subgroups.  Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|60112|6|Mentioned|p105-106, p109 Fig.2, p112, p116-117.  |||Displays syn-depositional extensional faulting.|||Includes Dresser and Panorama Formations; Euro, Mount Ada and Apex Basalts; North Pole Monzogranite.|Is unconformably overlain by Fortescue Group.||
19508|Warrawoona Group|60429|5|Briefly described|p6 Fig. 3, p8 Fig. 4.|Archean|Archean|Comprises Talga Talga Subgroup, the Duffer Formation and the Salgash Subgroup. Some mafic and ultramafic rocks in the discontinuous Yarrie Belt may be part of the Warrawoona Group. Age: <3430Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|60636|5|Briefly described|p11, p37|Archean|Archean|Overlain by Gorge Creek Group. Age: ~3.49-3.31Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|61111|5|Briefly described|p98, p96 Fig. 2, p111|Paleoarchean||Of the eastern Pilbara Craton.||||Includes the Panorama Formation. Unconformably overlain by the Strelley Pool Chert.||
19508|Warrawoona Group|61252|6|Mentioned|p65|||||||||
19508|Warrawoona Group|61253|5|Briefly described|p50 Fig. 1, p52 Fig. 2|Archean|Archean|Oldest member of the Pilbara Supergroup. Comprises four subgroups: Coonterunah, Talga Talga, Coongan and Salgash Subgroups. Previously incl. rocks of the former Kelly Subgroup, now part of upgraded Kelly Gp. Age: 3.52-3.43Ga. Geol.Prov: easternPilbara Cr.||||||07-NOV-08
19508|Warrawoona Group|61257|5|Briefly described|p353, p355 Tb. 1|Archean|Archean|Age: 3.51-3.43Ga.  Forms a good portion of the strutural dome known as North Pole Dome (Pilbara Craton) - dominantly weakly metamorphosed volcanic rocks (greenstones) and interbedded ultramafic, felsic and cherty horizons.||||||07-NOV-08
19508|Warrawoona Group|61264|5|Briefly described|p64 Fig. 2|||Of the Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||17-MAY-06
19508|Warrawoona Group|61266|4|Described|p55, p56, p58 Tb.1|Archean|Archean|Age: c. 3460 Ma. Unconformably overlies Coonterunah Group. Unconformably overlain by Sulphur Springs Group. Dominantly volcanic. Geologcial Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|61579|4|Described|p56|Archean|Archean|Unconformably overlies Coonterunah Group; unconformably overlain by Sulphur Springs Group. Age:  3.5-3.4Ga. Max. thickness: 15km.||||||07-NOV-08
19508|Warrawoona Group|61732|5|Briefly described|p25|Archean|Archean|Contains ancient microfossil assemblages.||||||07-FEB-11
19508|Warrawoona Group|62094|5|Briefly described|p235, p237|Archean|Archean|Includes host rocks for agate. Age: 3.48Ga; host rock tuff gives an age of 3477+/-5Ma (SHRIMP U-Pb). In the East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
19508|Warrawoona Group|62427|5|Briefly described|p1, p2-6, p14-15, p17-18 |Paleoarchean|Paleoarchean|Coppin Gap Greenstone Belt. 13 km thick.|~3490-3346 Ma (Beintima,2003; Nelson, 2001).||Includes the North Star and Euro Basalts; McPhee, Mount Ada, Duffer, Towers, Apex, Panorama and Wyman Formations.|Unconformably overlain by the Gorge Creek Group.|Silicified sedimentary rocks.|
19508|Warrawoona Group|62576|5|Briefly described|p619, p620 Fig. 3. |Archean|Archean|Metavolcanic rocks. Age: >/-3470Ma. Characterised by greenschist facies metamorphic mineral assemblages.||||||07-NOV-08
19508|Warrawoona Group|62979|5|Briefly described|p211, p213|||Includes the Coonterunah Subgp, North Star Basalt, Dresser Fm, Mount Ada and Apex Basalts, and Panorama Fm. Together with Kelly Group forms North Pole Dome. Overlain by the Kelly Group. Geol.Prov: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|63142|5|Briefly described|p487|Archean|Archean|Age: ca 3.51-3.43Ga. Overlain by the Kelly Group.||||||07-NOV-08
19508|Warrawoona Group|63245|5|Briefly described|p4, p19|Archean|Archean|Of the Pilbara Supergroup. Age: 3.51-3.42Ga. Consists of dominantly  volcanic and sedimentary rocks. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|63417|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Includes Coongan and Salgash Subgroups. Age: c.3465 to 3433Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup. Includes Talga Talga, Coongan and Salgash Subgroups, and several unassigned basalts, chert and schists. Geological Province: Pilbara Craton.||||||07-NOV-08
19508|Warrawoona Group|63441|4|Described|p4 Tb. 1|Archean|Archean|Of Pilbara Supergroup.Formerly comprised Salgash and Talga Talga Subgroups. Unconformably underlies either Kelly or Sulphur Springs Groups, or Gorge Creek, Croydon and Nullagine Groups. Age:3525-3426Ma. Max.thickness: ~12,000m. In the east Pilbara Terrane||||||07-FEB-11
19508|Warrawoona Group|63538|4|Described|p2 Fig. 1, p3 Fig. 2, p5, p7-9, p11-13|Archean|Archean|Of Pilbara Supergroup. Includes Panorama Fm, Apex Basalt, Duffer Fm, Mt Ada Basalt, Talga Talga Subgp and Coonterunah Subgp Age: 3525-3426 Ma. Thick: 12000 m. Geological Province: Pilbara Craton. Pillow and komatiitic basalt.||||||17-APR-13
19508|Warrawoona Group|63649|5|Briefly described|p200, p201|Archean|Archean|Of Pilbara Supergp. Includes Coucal, Dresser, McPhee and Duffer Fms, Apex Chert and Panorama Fm. Formerly included Strelley Pool Chert (now part of Kelly Gp). Unconformably overlain by Kelly Gp. Age: 3.52 - 3.43Ga. Geol.Prov: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|63854|5|Briefly described|p229 Fig.2, p230 |||||Unit in Pilbara Supergroup.|Includes the Panorama Formation.||Dominantly greenschist facies volcanic rocks.|
19508|Warrawoona Group|63866|5|Briefly described|p144|||||||Intruded by the Bridget Suite.||
19508|Warrawoona Group|64326|6|Mentioned|p72|Archean|Archean|||||||07-FEB-11
19508|Warrawoona Group|64327|5|Briefly described|p63|Archean|Archean|Age: c.3480-3325ma. Overlain by Budjan Creek Fm. Geol.Province: Pilbara Craton. Comprises greenschist-facies volcanic rocks and make up, to a large extent, the greenstone belt surrounding the Corunna Downs Granitoid Complex.||||||07-NOV-08
19508|Warrawoona Group|64328|4|Described|p54-58|||Contains Talga Talga, Salgash and Kelly Subgroups; formerly comprised only Talga Talga and Salgash Subgroups. Unconformably overlain by Budjan Creek Formation. Age: c.3490-3320Ma.||||||07-FEB-11
19508|Warrawoona Group|64405|5|Briefly described|p1, p16|Archean|Archean|Of the Pilbara Supergroup. Age: 3520-3427Ma. Geological province: East Pilbara Terrane.||||||07-FEB-11
19508|Warrawoona Group|64580|4|Described|map legend||Paleoarchean|Of Pilbara Supergroup. Mafic, ultramafic, and felsic volcanic and intrusive rocks, and sedimentary rocks; metamorphosed.||||||09-DEC-08
19508|Warrawoona Group|64621|5|Briefly described|Map legend|Archean|Archean|Includes the Salgash, Coongan and Talga Talga Subgroups. Comprehensive lithological details included.||||||07-NOV-08
19508|Warrawoona Group|64628|5|Briefly described|pp170-171, p184.  |Early Archean|Early Archean|With the Gorge Creek Group, forms the east-west striking Coppin Gap greenstone belt, northeast of Marble Bar. Generally youngs northward.|||Includes Talga Talga, Salgash and Kelley Subgroups; North Star, Mount Ada, Duffer, Towers, Panorama and Euro Formations.|||
19508|Warrawoona Group|64632|5|Briefly described|p201 Fig.1, p202, p204|Paleoarchean|Paleoarchean|East Pilbara terrane. Up to 12km thick.|3525-3426 Ma|Of the Pilbara Supergroup.||Unconformably overlain by the Kelly Group.|Consists of pillowed tholeiitic basalt, basaltic komatiite, with subordinate komatiite. Locally voluminous felsic volcanic rocks cap each (ultra) mafic to felsic volcanic cycle.|
19508|Warrawoona Group|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Includes Talga Talga, Salgash and Kelly Subgroups. Geological Province: Pilbara Craton.||||||07-FEB-11
19508|Warrawoona Group|64657|5|Briefly described|Map Legend|Archaean|Archaean|Includes Salgash Subgroup. Geological Province: Pilbara Craton.||||||
19508|Warrawoona Group|64747|5|Briefly described|p94 fig 1, p93, p96|Paleoarchean|Paleoarchean||3520-3420 Ma.|Pilbara Supergroup.|Includes Coonterunah Subgroup; North Star Basalt; Dresser, Duffer, Panorama Formations.|||
19508|Warrawoona Group|64936|5|Briefly described|map legend|Archean|Archean|Of Pilbara Supergroup. Includes Kelly Subgroup, Salgash Subgroup and Talga Talga Subgroup. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
19508|Warrawoona Group|65008|4|Described|p2, p5, p7, p8, p11-16, p24, p25, p41|Mesoarchean|Mesoarchean|East Pilbara Granite-Greenstone Terrane. Subdivided into 9 formations? Includes an unassigned unit of metamorphosed komatiitic basalt. Intruded by the Corunna Downs Granitoid Complex, Gobbos Granodiorite, Cooke[s] Creek Monzogranite, and Bridget Suite.|3200-2940 Ma|Of the Pilbara Supergroup|Includes Talga Talga Subgroup, Salgash Subgroup, and Kelly Subgroup.|Overlain by the Gorge Creek Group and Budjan Creek Formation. Unconformably overlain by the De Grey Group, Copper Gorge Formation, and Mount Roe Basalt. Intruded by the Bridget Suite.|Dominantly greenschist-facies volcanic rocks.|31-MAR-16
19508|Warrawoona Group|65415|5|Briefly described|p120 Fig.2.|Archean|Archean||c.3.4 - 3.5 Ma.|Unit in Pilbara Supergroup.||Is overlain unconformably by Wyman Formation.||
19508|Warrawoona Group|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Pilbara Supergroup.|Includes Kelly, Salgash and Talga Talga Subgroups.|||
19508|Warrawoona Group|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Also includes five unassigned units, mainly schists.||Of Pilbara Supergroup.|Includes Coongan and Salgash Subgroups.|||
19508|Warrawoona Group|65757|6|Mentioned|p81 Tb.2, p87|||In the Pilbara Craton. Includes Mount Ada Basalt, Apex Basalt.||||||
19508|Warrawoona Group|65825|5|Briefly described|pp5-10, p32.|Archean|Archean|Mount Elsie greenstone belt. Rocks in this unit were re-assigned (Van Kranendonk et al. 2004) to the Kelly Group (formerly Kelly Subgroup of the Warrawoona Group).||Unit in Pilbara Supergroup according to Van Kranendonk et al. (2001, 2002).|Includes Euro Basalt and Wyman Formation.|||
19508|Warrawoona Group|65827|3|Fully described|p6 Tb.1, p8, p9 Fig 3, p16-19, p27|Paleoarchean|Paleoarchean|Lipple (1975); redefined by Van Kranendonk et al. (2004). Of Pilbara Supergroup. Includes Apex Basalt, Panorama Formation; 4 subgroups including Coongan, Salgash and Talga Talga Subgroups. Formerly included Kelly Subgroup, Charteris Basalt. 3.53-3.43 Ga (Fig.3 has 3465-3427 Ma). Rocks correlated with this Group intrude the Mount Edgar Granitic Complex, Fig Tree Gneiss, Joorina Granodiorite, Bishop Creek Monzogranite, Kennel Granodiorite, Chessman Granodiorite.||||||
19508|Warrawoona Group|65828|6|Mentioned|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane.||Unit in Pilbara Supergroup.|Includes Kelly Subgroup, Wyman Formation and 2 unassigned units.|||
19508|Warrawoona Group|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. A major unit in Pilbara Supergroup. Includes Coonterunah, Talga Talga, Coongan and Salgash Subgroups, and an unassigned unit of amphibolite. Age shown from >3515 Ma to 3427 Ma.||||||
19508|Warrawoona Group|66118|4|Described|p146 Fig.1, p147-150, p158|||Pilbara Craton. East Pilbara Terrane. Shown as Warrowoona, Kelly, and Sulphur Springs Group in Fig.2.|c. 3515 Ma; 3525-3426 Ma; 3530-3430 Ma|Stratigraphically lowest in Pilbara Supergroup||Is unconformably overlain by Kelly Group.|Predominantly volcanics rocks.|
19508|Warrawoona Group|66122|5|Briefly described|p73-77, 86|Archean|Archean|Mount Goldsworthy greenstone belt, NE Pilbara Craton. Mis-spelt as Warrawona Group on p86.|3.52 - 3.42 Ga.|Pilbara Supergroup.|Euro Basalt, Panorama Formation, Strelley Pool Chert/Formation.|Is overlain by Farrel Quartzite.|See Constituents. Altered volcanic and volcaniclastic rocks; also contains basalt and komatiitic basalt; includes black vein chert.|
19508|Warrawoona Group|66217|3|Fully described|p1, p5, p6, pp8-10, p12, pp14-17, p35.|Paleoarchean|Paleoarchean|East Pilbara Terrane. Hosts a Ni-Cu deposit. Formerly Warrawoona Beds (Maitland 1905). Re-defined by Van Kranendonk et al. (2002). Sub-divided by Van Kranendonk et al. (2006a) into four Subgroups. Is a right-way-up, autochthonous succession, 5,000-15,000 m thick, affected by granitic diapirism, at its type section. Thin sedimentary horizons contain the oldest traces of life on Earth in the form of stromatolites, putative microfossils of controversial biogenicity, and organic carbonaceous material. Felsic volcanism was contemporaneous with intrusion by Callina and Tambina Supersuites.|3525-3426 Ma.|Unit in Pilbara Supergroup.|Includes Coonterunah, Talga Talga, Coongan and Salgash Subgroups.|Is intruded by Muccan Granitic Complex. Is unconformably overlain by Strelley Pool Formation.|Predominantly basaltic volcanic rocks; some felsic volcanics and sedimentary rocks.|
19508|Warrawoona Group|66664|5|Briefly described|p3-9.  |||East Pilbara Terrane. Felsic intrusive rocks; sericitized and silicified basaltic rocks.||Part of Pilbara Supergroup.|Includes Coonterunah, Talga Talga, Coongan and Salgash Subgroups; Mount Ada, Apex and North Star Basalts; Panorama Formation.|||
19508|Warrawoona 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.||||||
19508|Warrawoona Group|66745|4|Described|pp50-59.|Paleoarchean|Paleoarchean|Predominantly volcanic.|3525-3427 Ma.|Unit in Pilbara Supergroup.|Includes Coonterunah, Talga Talga, Coongan and Salgash Subgroups.|Is overlain by Strelley Pool Formation or, where that unit is absent, by Euro Basalt.||
19508|Warrawoona Group|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~3530-~3435 Ma estimated from Fig.11.|||||
19508|Warrawoona Group|67130|5|Briefly described|p13, p17,p62|Paleoarchean|Paleoarchean|At least 12km thick, deposited over a 100 Ma period. Regional unconformity present. Deposition was followed by a 75 Ma hiatus in volcanism, during which the regional unconformity formed and the Strelley Pool Formation was deposited.|3530 Ma - 3430 Ma|Pilbara Supergroup|Includes Coucal Formation, Duffer Formation, Panorama Formation, Dresser Formation, McPhee Formation, Apex Basalt, Mount Ada Basalt, North Star Basalt, Double Bar Basalt, Table Top Basalt|Unconformably overlain by Strelley Pool Formation, Kelly Group|Pillow basalt, komatiitic basalt,  komatiite, lesser felsic volcanic intervals also present (tuffs and dacite deposits). Quartz rich sandstone, volcaniclastics, carbonates and cherts.|
19508|Warrawoona Group|67197|5|Briefly described|p1-5, p7, p9, p14, p19, p22, p29, p33-34|Paleoarchean|Paleoarchean|See also p36. Pilbara Craton.|3525-3427 Ma.|Pilbara Supergroup.|Coonterunah, Talga Talga, Coongan, Salgash Subgroups.|Is overlain unconformably by Strelley Pool Formation.||
19508|Warrawoona Group|67201|4|Described|p7 Fig.4, p8, p10, see comments|||In northern Pilbara Craton, East Pilbara Terrane. Detrital zircons: 3724 Ma Panorama Formation (Thorpe et al., 1992). Lower part derived from crust older than 3560 Ma (isotopic data, Jahn et al. 1981). Page location continued: p12 Tb.1, p23-24, p68-69.|3525-3427 Ma|Pilbara Supergroup|Salgash Subgroup, Coongan Subgroup, Talga Talga Subgroup, Coonterunah Subgroup|Is erosionally overlain by Strelley Pool Formation (regional unconformity). Is unconformably overlain by Coondamar Formation.||
19508|Warrawoona Group|67269|5|Briefly described|p2-3, p6-7 Figs.3-4, p9, p12-14, p26|Paleoarchean|Paleoarchean|Van Kranendonk et al. (2004) renamed the Strelley Pool Chert as the Strelley Pool Formation, and moved it from this Group into Kelly Group.|3525-3427 Ma.|Pilbara Supergroup.|Coonterunah, Talga Talga, Coongan and Salgash Subgroups.|Is overlain unconformably by Strelley Pool Formation.||
19508|Warrawoona Group|67270|5|Briefly described|p2-4, p18|Paleoarchean|Paleoarchean|East Pilbara Terrane. Constitutes most of the Marble Bar greenstone belt. c.15km thick; composed almost entirely of volcanic formations.|3525-3427 Ma.|Pilbara Supergroup.|Salgash, Coongan, Talga Talga, Coonterunah Subgroup.|Is overlain unconformably by Strelley Pool Formation.||
19508|Warrawoona Group|67668|5|Briefly described|Fig. 2; p. 153-4, 156, 161, 163; Tb.1. ||Paleoarchean|East Pilbara Terrane, Pilbara Craton.|Deposited 3515 - 3420 Ma.|Pilbara Supergroup|Coucal, Double Bar, Dresser, Duffer, Panorama, Table Top Formations; North Star, Mount Ada and Apex Basalts; "Apex chert".|Underlies the Strelley Pool Formation|Consists mostly of mafic volcanic rocks interspersed with thin chert horizons, felsic volcanic rocks and volcaniclastics.|
19508|Warrawoona Group|68035|4|Described|p287, p286 Fig 3|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Erosional unconformity of ~75 million years to overlying Kelly Group|3.53 Ga - Min age ~3427 Ma|Of Pilbara Supergroup.|Includes Coonterunah Subgroup, Talga Talga Subgroup, Coongan Subgroup, Salgash Subgroup.|Unconformably overlain by Kelly Group,  Strelley Pool Formation. Associated with Callina Supersuite, Tambina Supersuite.||
19508|Warrawoona Group|68280|6|Mentioned|p1, p4, p11, p13, p16, p19, p35||||||Includes Coonterunah Subgroup, Talga Talga Subgroup, Coongan Subgroup, Salgash Subgroup|||18-JAN-23
19508|Warrawoona Group|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Coonterunah Subgroup, Coongan Subgroup, Salgash Subgroup, McPhee Formation, North Star Basalt.|||10-JUN-14
19508|Warrawoona Group|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Terminated by Warrawoona Event (3430-3410 Ma).|Older than 3410 Ma.|Of the Pilbara Supergroup|Includes Salgash Subgroup.|||03-DEC-14
19508|Warrawoona Group|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|> 3350 Ma|Of the Pilbara Supergroup.|Includes Salgash Subgroup, Coongan Subgroup, Talga Talga Subgroup, Coonterunah Subgroup.|||
19508|Warrawoona Group|68284|5|Briefly described|p4-7, 20|Paleoarchean|Paleoarchean|Pilbara Craton. Locally, pre-3430 Ma erosion has removed 4-8km of this succession.|3530-3427 Ma.|Pilbara Supergroup.|Coonterunah, Talga Talga, Coongan, Salgash, Subgroups.|Is overlain by Strelley Pool Formation.|Predominantly basalt; also significant sedimentary units.|
19508|Warrawoona Group|68312|5|Briefly described|p103-104|Archean|Archean|North Pole Dome, Pilbara Craton.|||Panorama Formation.||Pillowed basaltic greenstones, thick cherts and interbedded barites; felsic volcanic/volcaniclastic rocks, sandstone/bedded chert.|
19508|Warrawoona Group|69012|5|Briefly described|Map Legend|Archean|Archean|East Pilbara Terrane.||Of the Pilbara Supergroup.|Includes the Salgash Subgroup, Coongan Subgroup, and Talga Talga Subgroup.|||
19508|Warrawoona Group|69013|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Of the Pilbara Supergroup.|Includes the Coonterunah Subgroup and Double Bar Formation.|||30-APR-14
19508|Warrawoona Group|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Of the Pilbara Supergroup.|Includes Salgash, Coongan, Talga Talga and Coonterunah Subgroups.|||02-MAY-14
19508|Warrawoona Group|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Fine grained felsic volcanic rock, gabbro, dolerite, basalt, komatiitic basalt, anorthositic metagabbro, pyroxenite.Age derived from samples of volcaniclastic sandstone and porphyritic rhyolite tuff an (169026.1.pdf, 168996.1.pdf) and is interpreted as the ages of sandstone deposition and igneous crystallisation of the felsic volcanic precursor to the altered tuff.|3458 +/- 9 Ma -3477  +/- 5 Ma (SHRIMP)|Pilbara Supergroup|Includes Salgash Subgroup, Coongan Subgroup, Talga Talga Subgroup||Schist, quartzite, calc-silicate gneiss, amphibolite, metagabbro, silicified komatiitic basalt and associated quartz vein breccia. Metaperidotite, serpentinite, serpentine-talc schist, ultramafic schist and chert.|
19508|Warrawoona Group|69185|4|Described|500k_geologyp08_lut.csv||Paleoarchean|Geological Province: Pilbara Craton.||Unit of Pilbara Supergroup.|Includes Coongan Subgroup, Coonterunah Subgroup, Salgash Subgroup, Talga Talga Subgroup, Strelley Pool Chert.||Mafic, ultramafic, and felsic volcanic and intrusive rocks, and sedimentary rocks; metamorphosed|
19508|Warrawoona Group|69301|4|Described|p5 Fig.3, p9 Tb.1, p11, p19, p21 Fig.8|||Pilbara Craton. East Pilbara Terrane.|3520-3430 Ma; 3525-3430 Ma from unit ages|Pilbara Supergroup|Salgash Subgroup, Coongan Subgroup, Talga Talga Subgroup, Coonterunah Subgroup|Is unconformably overlain by Kelly Group (regional). Overlain by Strelley Pool Formation.|Includes BIF.|
19508|Warrawoona Group|69548|6|Mentioned|p2|||Pilbara region.||||Is overlain by Sulphur Springs Group. Is intruded by Strelley Granite.|Mafic volcanic rocks.|
19508|Warrawoona Group|69566|5|Briefly described|p236-238, 241, 248|||East Pilbara Granite-Greenstone Terrane. Approx. 12km thick.|3508-3445 Ma.||Mount Ada, Apex Basalts; Duffer, Panorama FXs.|Is overlain unconformably by Kelly Group.||
19508|Warrawoona Group|69569|6|Mentioned|p284-285|||Marble Bar greenstone belt, East Pilbara Terrane.|3525-3170 Ma.||Apex, Mount Ada, North Star Basalts; Dresser, Duffer, Panorama Formations.|||
19508|Warrawoona 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. Sample GSWA 168996 (porphyritic rhyolite tuff) yielded an interpreted igneous crystallisation age of 3277+\-5 Ma for the volcanic precursor of the tuff (weighted mean 207Pb/206Pb). Sample GSWA 169026 (volcaniclastic metasandstone) yielded an interpreted maximum depositional age of 3458+\-9 Ma for 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, 250k_interpgeol_lut.csv.|3515-3427 Ma (inferred)|Unit of Pilbara Supergroup.|Includes Coongan Subgroup, Coonterunah Subgroup, Salgash Subgroup, Talga Talga Subgroup.||Amphibolite, basalt and komatiitic basalt, calc-silicate gneiss, chert, metamorphose gabbro and dolerite, metaperidotite, pyroxenite, quartzite, schist and ultramafic schist, silicified komatiitic basalt.|
19508|Warrawoona Group|69740|5|Briefly described|p651, 663, 673, 676|Paleoarchean|Paleoarchean|Suprasubduction zone-type ophiolite; backarc to forearc plume magmatism.|3.53-3.43 Ga.|Pilbara Supergroup.|||Mainly basaltic pillow lava, minor felsic and ultramafic lavas, chert layers.|
19508|Warrawoona Group|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|||Coonterunah Subgroup; Dresser, Mount Ada, Duffer, Panorama Formations; Marble Bar, Apex Cherts; Apex Basalt.|||
19508|Warrawoona Group|70022|6|Mentioned|p113-115|||East Pilbara Terrane.|3525-3426 Ma.||Coonterunah, Talga Talga, Coongan, Salgash Subgroups.|Is overlain unconformably by Strelley Pool Formation.||
19508|Warrawoona Group|70507|5|Briefly described|p429-431,442|Archean|Archean|Geological province: Pilbara Craton.||Unit of Pilbara Supergroup.|Includes Panorana, Duffer and Dresser formations, Mount Ada Basalt and North Star Basalt.|||
19508|Warrawoona Group|70729|6|Mentioned|p163-164|||Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Pilbara Supergroup.|Includes Salgash, Coongan, Talga Talga and Coonterunah subgroups, and Apex Basalt.|||
19508|Warrawoona Group|70733|6|Mentioned|p104-105, 120|||Pilbara Craton.|3530-3426 Ma.|Pilbara Supergroup.|Coonterunah, Talga Talga, Coongan, Salgash Subgroups.|||
19508|Warrawoona Group|70775|5|Briefly described|p2, p12, p70, p100|||Previously this group was effectively equivalent to the present Pilbara Supergroup (all the rocks contained within it were assigned to the Warrawoona Group-p100). Also includes the Dresser Formation, McPhee Formation, North Star Basalt, Double Bar Formation, Coucal Formation and the Table Top Formation..|c. 3430-3525 Ma|Pilbara Supergroup|Includes the Coonterunah Subgroup, Panorama Formation, Apex Basalt, Duffer Formation, Mount Ada Basalt.|Unconformably overlain by the Strelley Pool Formation.||
19508|Warrawoona Group|70826|6|Mentioned|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Pilbara Supergroup||Unconformably overlain by the Kelly Group.||12-MAY-20
19508|Warrawoona Group|70834|6|Mentioned|p298, 310|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton. 10-15 km thick. Hydrothermal production of micas and later alteration to vermiculite, followed by exfoliation, has produced abiotic filamentous microstructures instead of putative ""microfossils"" in the Apex chert.|||Apex Basalt, Marble Bar Chert.||Volcano-sedimentary succession with minor interstratified chert, barite, carbonate and volcaniclastic units.|
19508|Warrawoona Group|70884|5|Briefly described|p123,p125, 128,133-134,136-137|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Experienced southward tilting as a result of crustal uplift and doming from Muccan Granitic Complex emplacement.||Unit of Pilbara Supergroup.|Includes Salagah, Coongan, Talga Talga and Coonterunah subgroups.|Overlain unconformably by Strelley Pool Formation.||16-AUG-19
19508|Warrawoona Group|71137|6|Mentioned|p2, 4-5|Archean|Archean|||||Is overlain unconformably by Farrel Quartzite (Gorge Creek Group).||
19508|Warrawoona Group|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||komatiitic (high-mg) basalt, basalt, gabbro, dolerite, mafic schist, ultramafic schist|
19508|Warrawoona Group|71487|5|Briefly described|p127-128|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3530-3427 Ma|Unit of Pilbara Supergroup.|Includes Salgash, Coongan, Talga Talga and Coonterunah subgroups.|Overlain unconformably by Strelley Pool Formation.||
19508|Warrawoona Group|71808|6|Mentioned|p97|||||||||
19508|Warrawoona Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province. Mafic + felsic volcanic rocks w minor sedimentary + intrusive rocks. Basalt + komatiitic basalt; locally silicified or schistose. Basalt; massive or pillowed, locally variolitic. All 3 metamorphosed. Amphibolite derived from mafic intrusive/extrusive rock. Ultramafic schist. Serpentized peridotite + komatiite; includes serpentinite + tremolite-chlorite-serpentine-carbonate schist.||Pilbara Supergroup|Includes Nob Well Intrusion, Strutton Intrusion, Gap Intrusion and 5 unnamed units.||Mafic and felsic volcanic rocks with minor sedimentary and intrusive rocks; metamorphosed.|
19508|Warrawoona Group|72064|5|Briefly described|p65-66,76|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Mostly eroded on the East Strelley Greenstone Belt prior to deposition of the Strelley Pool Formation.|c. 3515-3427 Ma|Unit of Pilbara Supergroup.|Includes Panorama Formation, Apex Basalt, Duffer Formation, Mount Ada Basalt, McPhee Formation, Dresser Formation, North Star Basalt, Double Bar Formation, Coucal Formation and Table Top Formation.|Overlain unconformably by Strelley Pool Formation. Intruded by the Carlindi Granite.||28-JAN-20
19508|Warrawoona Group|72251|5|Briefly described|p52-55|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|3525-3426 Ma|Unit of Pilbara Supergroup.|Includes Salgash, Coongan, Talga Talga and Coonterunah subgroups.|Lowermost unit of Pilbara Supergroup. Overlain unconformably by Kelly Group.||
19508|Warrawoona Group|72668|4|Described|p3-7, p9-10, p13, p18, p20, p24-27, p30|||East Pilbara Terrane. At least 12km thick, deposited over 100myr as a result of continuous volcanism. Volcanism occurred in several mafic-felsic cycles of c. 15 Myr duration capped by thin sedimentary rocks.Deposition occurred predominantly under submarine conditions in what is interpreted to be an oceanic-type plateau erupted on a basement of older continental crust. Geochemistry, structure and metamorphism are discussed.|3525-3426 Ma|Pilbara Supergroup|Includes the Salgash Subgroup, Coongan Subgroup, Talga Talga Subgroup and the Coonterunah Subgroup.|Unconformably overlain by the Kelly Group.|Pillow basalt and komatiitic basalt and minor komatiite. Lesser felsic volcanic intervals are restricted to tuffaceous horizons.|
19508|Warrawoona Group|73160|5|Briefly described|p1, p2 Fig.1, p3-4, p8 Fig.6|Archean|Archean|Pilbara Craton, East Pilbara Terrane. Phrenite-pumpellyite to lower greenschist facies metamorphism, amphibolite grade metamorphism restricted to contact metamorphic aureoles of granitic intrusions|||Dresser Formation, North Star Basalt, Mount Ada Basalt, Panorama Formation.||Volcano-sedimentary group. Includes greenstones, felsic volcanic rocks interbedded with basaltic units.|
19508|Warrawoona Group|73598|5|Briefly described|p1207, 1209, 1212|Paleoarchean|Paleoarchean|East Pilbara Terrane. ~15 km thick.|c.3530-3430 Ma.|Pilbara Supergroup.|Coonterunah, Talga Talga, Coongan, Salgash Subgroups.|Is overlain unconformably by Strelley Pool Formation.|Dominantly basalt sequence.|
19532|Warrimbah Conglomerate|22741|5|Briefly described|P31, Table3 P10||Cenozoic|||||||19-NOV-08
19532|Warrimbah Conglomerate|22767|5|Briefly described|Table3 P12, P24||Cenozoic|||||||19-NOV-08
19532|Warrimbah Conglomerate|30287|6|Mentioned|p16|||Quaternary age||||||
19532|Warrimbah Conglomerate|30525|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19532|Warrimbah Conglomerate|30533|4|Described|p30|||On Table 9||||||
19532|Warrimbah Conglomerate|31078|6|Mentioned|p103|||||||||
19532|Warrimbah Conglomerate|32648|6|Mentioned|p32|||Pleistocene||||||
19532|Warrimbah Conglomerate|36225|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
19532|Warrimbah Conglomerate|36634|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
19532|Warrimbah Conglomerate|36890|4|Described|p357|||||||||
19532|Warrimbah Conglomerate|38263|6|Mentioned|p13|||||||||
19532|Warrimbah Conglomerate|38878|6|Mentioned|Map legend|Pliocene|Miocene|Miocene - Pleistocene||||||
19532|Warrimbah Conglomerate|39796|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19532|Warrimbah Conglomerate|41158|6|Mentioned|Plate 3|||||||||
19532|Warrimbah Conglomerate|42710|5|Briefly described|map legend|Tertiary||||||||
19532|Warrimbah Conglomerate|42811|5|Briefly described|p47|||||||||
19532|Warrimbah Conglomerate|43281|5|Briefly described|Map legend||Tertiary|||||||
19532|Warrimbah Conglomerate|43563|6|Mentioned|Fig2,p5,16|Pleistocene|Pliocene|||||||
19532|Warrimbah Conglomerate|43818|6|Mentioned|Fig.2.p39||Cenozoic|||||||19-NOV-08
19532|Warrimbah Conglomerate|44143|4|Described|p.429 Table 4-19|Cainozoic|Cainozoic|?10 m thick; pebble and cobble gravel, fluvial. Fossil kangaroo and crocodile bones at Alligator Dam may come from this Formation. Mainly confined to within 15 km of Fitzroy River.||||||24-NOV-17
19532|Warrimbah Conglomerate|44403|2|Defined|opp.p.6, Tb.1|||E/51-12. See Casey J.N. 1958b, for more details.||||||
19532|Warrimbah Conglomerate|44404|14|Not recorded|map legend||Tertiary|||||||
19532|Warrimbah Conglomerate|44998|2|Defined|p197-8|||(E51-11,12). See also p194, map.||||||
19532|Warrimbah Conglomerate|45153|3|Fully described|App.11-169|||See also Table 1||||||
19532|Warrimbah Conglomerate|45158|3|Fully described|p10|||See P34||||||
19532|Warrimbah Conglomerate|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Age: ~17-~13.5Ma. Thickness: 10m. Geological Province: Fitzroy Graben.||||||
19532|Warrimbah Conglomerate|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Unconsolidated fluvial cobble and minor pebble conglomerate; brown clasts, and fossiliferous in places|
19542|Warrulinya Suite|23783|5|Briefly described|p100|Archean|Archean|||||||07-NOV-08
19542|Warrulinya Suite|23807|6|Mentioned|p141|||Geological Province: Pilbara Craton.||||||
19542|Warrulinya Suite|24590|5|Briefly described|p44 Fig. 2.5|Archean|Archean|Identified as one of the trondhjemite-tonalite suites of the Mount Edgar Granitoid Complex. Age: 3.31Ga. See also Warulinya Suite.||||||07-FEB-11
19542|Warrulinya Suite|41938|4|Described|p15|||||||||
19542|Warrulinya Suite|69041|4|Described|p4, p18-p19|Paleoarchean|Paleoarchean|Pilbara Craton, of the Mount Edgar Igneous Complex (which is used in a province sense). Forms the western most elliptical body of the Complex. Not metamorphosed beyond greenschist facies. Outcrops vary from scattered to abundant boulders on low hills to low slabs. Contains three unnamed units.|3466 +/- 2Ma (SHRIMP U-Pb, Nelson, 1998)||||Medium- to coarse-grained, biotite-hornblende granodiorite to biotite monzogranite ranging from sparsely developed feldspar porphyritic to seriate and locally leucocratic.|21-JUN-19
19542|Warrulinya Suite|69167|6|Mentioned|GA_geochron.csv|Archaean|Archaean|||||||
19549|Warton Sandstone|22440|6|Mentioned|p5|||||||||
19549|Warton Sandstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.||||||07-NOV-08
19549|Warton Sandstone|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Kimberley Group.||||||
19549|Warton Sandstone|23383|5|Briefly described|p19, p18 Tb.2|||Of Kimberley Group. White to purple, massive to blocky, thin-bedded, fine- to medium-grained quartz sandstone. Conformably overlain by Elgee Siltstone; conformably overlies Carson Volcanics. Max thickness: 300 m.  Geological Province:  Kimberley Basin.||||||25-JAN-05
19549|Warton Sandstone|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Kimberley Group. White to purple, massive to blocky, quartz sandstone,; minor feldspathic sandstone. Geological Province: Kimberley Basin.||||||07-NOV-08
19549|Warton Sandstone|23621|6|Mentioned|p31|||||||||
19549|Warton Sandstone|23722|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Parent: Kimberley Group.  Max. thickness: 500m.   Geological Province: Kimberley Basin||||||07-NOV-08
19549|Warton Sandstone|24173|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|May form part of the undivided Kimberley Group||||||07-NOV-08
19549|Warton Sandstone|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Geological Province: Kimberley Basin.||||||07-NOV-08
19549|Warton Sandstone|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Age: <1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
19549|Warton Sandstone|29380|4|Described|Table 2|||Carpentarian.||||||
19549|Warton Sandstone|29693|6|Mentioned|p106|||||||||
19549|Warton Sandstone|29946|6|Mentioned|p253|||||||||
19549|Warton Sandstone|30097|6|Mentioned|p151|||See also Table 23||||||
19549|Warton Sandstone|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|30533|4|Described|p18|||On Table 3||||||
19549|Warton Sandstone|30636|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|30893|5|Briefly described|p205|||Lithology. Carpentarian.||||||
19549|Warton Sandstone|30894|5|Briefly described|p250|||Carpentarian||||||
19549|Warton Sandstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|30896|4|Described|p17|||||||||
19549|Warton Sandstone|30897|6|Mentioned|p13|||Stratigraphy||||||
19549|Warton Sandstone|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19549|Warton Sandstone|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
19549|Warton Sandstone|31662|6|Mentioned|Fig. 1|||||||||
19549|Warton Sandstone|32660|5|Briefly described|Table 3|||||||||
19549|Warton Sandstone|32662|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|32663|4|Described|Table 1|||Carpentarian||||||
19549|Warton Sandstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|32728|5|Briefly described|p38|||Mention Table 5||||||
19549|Warton Sandstone|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|34137|4|Described|Table 1||Carpentarian|Carpentarian. Part of Kimberley Group.||||||
19549|Warton Sandstone|34190|4|Described|Table 1|||||||||
19549|Warton Sandstone|34462|4|Described|Table 1|||Carpentarian||||||
19549|Warton Sandstone|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19549|Warton Sandstone|36551|4|Described|p33|||||||||
19549|Warton Sandstone|36885|4|Described|p185|||||||||
19549|Warton Sandstone|37228|6|Mentioned|p44|||See also Fig.2.||||||
19549|Warton Sandstone|37462|6|Mentioned|Fig.4.9|||||||||
19549|Warton Sandstone|39116|6|Mentioned|p134|||||||||
19549|Warton Sandstone|41158|5|Briefly described|Fig.9|||Mention p24||||||28-MAR-23
19549|Warton Sandstone|41703|6|Mentioned|p229|||See also Fig.2||||||
19549|Warton Sandstone|42149|6|Mentioned|Table 1 P709|||||||||
19549|Warton Sandstone|42710|5|Briefly described|map legend|Proterozoic||||||||
19549|Warton Sandstone|42811|5|Briefly described|p23|||of Kimberley Group||||||
19549|Warton Sandstone|42814|4|Described|p14|||of Kimberley Group||||||
19549|Warton Sandstone|42815|5|Briefly described|map|Proterozoic||||||||
19549|Warton Sandstone|42977|5|Briefly described|p275|||||||||
19549|Warton Sandstone|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Group.||||||
19549|Warton Sandstone|43652|6|Mentioned|Fig.5,p383|||||||||
19549|Warton Sandstone|44140|5|Briefly described|p295, p298 fig 4-5|Paleoproterozoic|Paleoproterozoic|60-600 m thick.||Kimberley Group||Intruded by Wotjulum Porphyry|Quartz and feldspathic sandstone; minor shale; cross-beds, ripple marks, clay pellets.|
19549|Warton Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
19549|Warton Sandstone|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberely Group. White to purple, massive to blocky quartz sandstone; minor feldspathic sandstone. Geological Province: Kimberley Basin.||||||07-NOV-08
19549|Warton Sandstone|44286|5|Briefly described|Map legend|||||||||
19549|Warton Sandstone|44363|5|Briefly described|p.6,10,11,12|||(Carpentarian) Kimberley Group.||||||
19549|Warton Sandstone|44364|14|Not recorded|map legend|||||||||
19549|Warton Sandstone|44366|14|Not recorded|p.15, Table 2||Carpentarian|Part of Kimberley Group.||||||
19549|Warton Sandstone|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Kimberley Group.||||||
19549|Warton Sandstone|44397|14|Not recorded|p.17, Table 2||Carpentarian|Kimberley Group.||||||
19549|Warton Sandstone|44398|14|Not recorded|map legend||Carpentarian|||||||
19549|Warton Sandstone|44694|5|Briefly described|Map Legend||Proterozoic|||||||
19549|Warton Sandstone|45047|5|Briefly described|p28|||||||||
19549|Warton Sandstone|45077|6|Mentioned|p7|||||||||
19549|Warton Sandstone|48931|3|Fully described|p54|||||||||
19549|Warton Sandstone|60714|5|Briefly described|p112, p113 Fig.2, p118. |Statherian|Statherian|275-365 m thick. Age by McNaughton et al. (1999). Youngest detrital zircon 1786 +/- 14 Ma.|1704 +/- 7 Ma (U-Pb diagenetic xenotime).|Unit in Kimberley Group.||Overlies Carson Volcanics. Is overlain by Elgee Siltstone.|Mature, quartzose and feldspathic sandstone.|
19549|Warton Sandstone|61571|5|Briefly described|p657|Paleoproterozoic|Paleoproterozoic|Oldest unit in the Spider impact structure forming the central dome - of mature, medium-grained arenite. Overlies Carson Volcanics; overlain by Elgee Siltstone. Max. thickness in impact structure: 500m. Age: 1704+/-7Ma (SHRIMP U-Pb) and 1786+/-14Ma.||||||07-NOV-08
19549|Warton Sandstone|64329|6|Mentioned|p28|||Heavy mineral concentrations are present, including thorium. Exploration in this and Warton Sandstone constitute the Durack Range Uranium project of the East Kimberley region in WA.||||||29-JUL-08
19549|Warton Sandstone|64580|4|Described|map legend||Paleoproterozoic|Of Kimberley Group. Sandstone.||||||09-DEC-08
19549|Warton Sandstone|64748|4|Described|p268, p269 Fig 2,p269 Tb.1, p275|Statherian|Statherian|U-Pb detrital zircon age 1786+/-14Ma; diagenetic xenotime ages 1704+/-7Ma; of Kimberley Group; includes Buckland Point Member; quartzose and feldspathic sst, minor mudstone, clay pellets; 60-600m thick; underlies Elgee Sandstone; overlies Carson Volcanics||||||
19549|Warton Sandstone|67563|5|Briefly described|p120, p121, p122 Fig.2, p130, p131|Statherian|Orosirian|Xenotime and youngest detrital zircon ages by McNaughton et al. (1999). An additional youngest detrital zircon age by Kirkland et al. (2010) is also included.|1704 +/- 7 Ma(xenotime); 1786 +/- 14 (detr).|Of the Kimberley Group.||||20-JAN-17
19549|Warton Sandstone|68078|5|Briefly described|p2, p4 figure 2, p6-8, p24|Paleoproterozoic|Paleoproterozoic|Age is of approximate depositional age. See also p10, p19, p21 figure 14.|1704 Ma +/- 7 Ma (SHRIMP)|Kimberley Group||Overlies Carson Volcanics, overlain by Elgee Siltstone, Pentecost Sandstone, Intruded by Hart Dolerite|Sandstone.|13-SEP-22
19549|Warton Sandstone|68244|6|Mentioned|p662|||Kimberley Basin.||||||
19549|Warton Sandstone|68992|5|Briefly described|p498, p498 Fig.1, p499, pp504-507||Statherian|Kimberley Basin. Diagenetic xenotime age of 1704 +/- 7 Ma (McNaughton et al. 1999). Youngest detrital zircon age.|<1786 +/- 14 Ma (McNaughton et al 1999).|Of the Kimberley Group.||Underlain by the King Leopold Sandstone.||
19549|Warton Sandstone|69003|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|U-Pb zircon maximum depositional age. Also shown as having a 1704 Ma U-Pb xenotime age.|<1786 Ma.|Kimberley Group.||Overlies Carson Volcanics. Is overlain by Elgee Siltstone. Intruded by Wotjulum Porphyry.||
19549|Warton Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. Age from analyses done in 2010. See 182104.1.pdf.|Max.deposit 1806+/-28 Ma U/Pb SHRIMP|Kimberley Group||Conformably overlies Carson Volcanics|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone|21-JUL-15
19549|Warton Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|||Kimberley Group|||White to buff quartz sandsotne and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|69585|4|Described|p3-5, p8-9, p12, p17, p20-21, p27, p31|Orosirian|Orosirian|Tidal to shallow-marine deposits. Hf isotope data and diagram.|1862 +/- 17 Ma (maximum depositional age).|Kimberley Group.||Conformably overlies Carson Volcanics. Is overlain conformably by Elgee Siltstone.|Medium-grained, well-sorted, quartz-dominated sandstones, feldspathic sandstones (subarkose or arkose), with minor micaceous siltstone. Sandstones are commonly cross-bedded.|
19549|Warton Sandstone|69597|6|Mentioned|p4|||||||||
19549|Warton Sandstone|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Minimum depositional age of 1740+\-6 Ma, based on magmatic crystallisation age of Wotjulum Porphyry that intrudes Elgee Siltstone. Weighted mean 207Pb*/206Pb* date of 1862+\-17 Ma (interpreted maximum depositional age, geochron files), compared withreported MDA of 1786+\14 Ma provided by McNaughton et al. (1999). Contain zircon age components at c. 1900-1800 and 2500-2400 Ma (McNaughton et al., 1999; Kirkland et al., 2010). Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1835-1740 Ma (Inferred)|Unit of Kimberley Group.|Includes Buckland Point Member.|Overlain by Elgee Siltstone. Underlain conformably by Carson Volcanics.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone|
19549|Warton Sandstone|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, Kimberley Craton.||Unit in Kimberley Group.||Overlies Carson Volcanics.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin; North Australian Craton.||Kimberley Group.||Overlies Carson Volcanics. Is overlain by Elgee Siltstone.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Upper Kimberley Group.|Buckland Point Member.|Overlies Carson Volcanics. Is overlain by Elgee Siltstone.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1740-1835 Ma|Kimberley Group|||White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|70731|5|Briefly described|p270|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||Unit of Kimberley Group.||Underlain by Carson Volcanics.||
19549|Warton Sandstone|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|Buckland Point Member.|Overlies Carson Volcanics. Is overlain by Elgee Siltstone.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.||Overlies Carson Volcanics. Is overlain by Elgee Siltstone.Intruded by Hart Dolerite.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|10-NOV-16
19549|Warton Sandstone|70812|5|Briefly described|p6|Statherian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1800 Ma|Kimberley Group, Lower||||
19549|Warton Sandstone|70851|5|Briefly described|p4-p5, p34|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1800-1775 Ma|Kimberley Subgroup, Lower||Overlies the Carson Volcanics. Overlain by the Elgee Sandstone.||
19549|Warton Sandstone|71267|4|Described|GEOL_LUT_CSV files|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). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1835-1740 Ma (inferred)|Unit of Kimberley Group.||Underlain conformably by Carson Volcanics. Intruded by Wotjulum Porphyry.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone|
19549|Warton Sandstone|71281|4|Described|p421, p423|Paleoproterozoic|Paleoproterozoic|Gellatly and Derrick (1967). Kimberley Basin. Up to 500m thick. c.1704 Ma age from metamorphic xenotime.|1806 +/- 28 Ma (maximum depositional age).|Kimberley Group.||Overlies Carson Volcanics. Is overlain by Elgee Siltstone.|Massive to blocky, cross-bedded, medium-grained quartz sandstone, commonly white to purple, and minor feldspathic sandstone with a 1-5m thick basal siltstone with siliceous stromatolites.|
19549|Warton Sandstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.||Overlies Carson Volcanics. Is overlain by Teronis Member (Elgee Siltstone), and unconformably by Walsh Tillite.|White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group, upper|||White to buff quartz sandstone and feldspathic sandstone; siltstone interbeds; minor hematitic sandstone.|
19549|Warton Sandstone|72490|5|Briefly described|p3-4|||Maximum thickness of 500 m.||Kimberley Group|||Cross-bedded, commonly white to purple, medium-grained quartz sandstone and minor feldspathic sandstone. Locally there is a 1-5m thick siltstone between the volcanic rocks and sandstone with siliceous stromatolites.|
19550|Warubuyu Basalt|30388|4|Described|Table 1|||Table 1 P10. Middle Proterozoic age.||||||
19550|Warubuyu Basalt|30390|4|Described|p76|||||||||
19550|Warubuyu Basalt|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Cassidy Group.||||||
19550|Warubuyu Basalt|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
19550|Warubuyu Basalt|36551|6|Mentioned|Table 31|||||||||
19550|Warubuyu Basalt|36886|4|Described|p198|||||||||
19550|Warubuyu Basalt|67375|5|Briefly described|p38 Table 1, p49. |Mesoproterozoic|Mesoproterozoic|||Unit in Cassidy Group.||Overlies Thomas Rhyolite. Is overlain by Hilda Rhyolite.||
19550|Warubuyu Basalt|67553|5|Briefly described|p40,51-52,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Underlain by an unnamed sedimentary siliciclastic sequence and intercalated with a separate siliciclastic sequence; the entire package is termed the Warubuyu Formation (this study).||Unit of Cassidy Group.||Overlain by Hilda Rhyolite. Underlain by Thomas Rhyolite.||
19550|Warubuyu Basalt|68995|5|Briefly described|p7 Fig.3, p9 Tb. 1, p18, p49 Fig.25|Stenian|Stenian|Estimated 300m thick.||Cassidy Group||Overlies the Thomas Rhyolite. Overlain by the Hilda Rhyolite.|Basaltic lava flows.|
19550|Warubuyu Basalt|69091|5|Briefly described|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
19550|Warubuyu Basalt|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample description: metabasalt. Mentioned in GEOCHRON/174691.1.pdf and 174690.1.pdf.||Cassidy Group|||Basalt and basaltic andesite, interlayered with volcanolithic mudstone, siltstone, sandstone, conglomerate, and laminated microbialite; local hyaloclastite; epidotized|
19550|Warubuyu Basalt|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
19550|Warubuyu Basalt|70095|5|Briefly described|p16-17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of basaltic package: 0.2km.||Unit of Cassidy Group.||Overlain by Hilda Rhyolite. Underlain by Thomas Rhyolite.||
19550|Warubuyu Basalt|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The two facies are mapped separately.||Cassidy Group.||Overlies Thomas Rhyolite. Is overlain by Hilda Rhyolite.|Massive to amygdaloidal basalt and basaltic andesite, interlayered with volcanolithic mudstone, siltstone, ripple cross-laminated sandstone, conglomerate and laminated microbialite, local hyaloclastite, epidotised; laminated siltstone and sandstone.|
19550|Warubuyu Basalt|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Cassidy Group|||Massive to amygdaloidal basalt and basaltic andesite, includes interlayers of volcanolithic mudstone, conglomerate and of fine-grained, laminated siltstone sandstone and microbialite with ripple marks or laminar cross bedding; epidotized.|
19550|Warubuyu Basalt|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, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Basalt and basaltic andesite, amygdaloidal to massive; interlayered; and fine-grained sandstone; epidotized; laminated siltstone and sandstone, interlayered volcanilithic mudstone, siltstone, sandstone, conglomerate, microbialite, hyaloclastite.|
19550|Warubuyu Basalt|71211|6|Mentioned|p216|||||Cassidy Group||||
19550|Warubuyu 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). 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.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Basalt and basaltic andesite; massive to amygdaloidal; fine-grained- laminated sandstone and siltstone, volcanolithic mudstone, conglomerate, microbialite, local hyaloclastite.|
19550|Warubuyu Basalt|72443|6|Mentioned|p738-739, p748|||Talbot Sub-basin.||Cassidy Group||||
19557|Wataru Gneiss|24197|6|Mentioned|p98|||Only named unit of Birksgate Complex. In the Birksgate Range. Geological Province: Musgrave Block.||||||07-FEB-11
19557|Wataru Gneiss|24496|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Of Birksgate Complex. Massive orthogneiss to gneiss to weakly layered gneiss. Geological Province: Musgrave Block.||||||
19557|Wataru Gneiss|24499|6|Mentioned|Map legend|||||||||
19557|Wataru Gneiss|30923|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19557|Wataru Gneiss|31965|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19557|Wataru Gneiss|33478|5|Briefly described|p451|||||||||
19557|Wataru Gneiss|35308|5|Briefly described|p451|||||||||
19557|Wataru Gneiss|40229|5|Briefly described|p28|||||||||
19557|Wataru Gneiss|40910|6|Mentioned|p7|||||||||
19557|Wataru Gneiss|40911|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early-Middle Proterozoic||||||07-NOV-08
19557|Wataru Gneiss|43052|5|Briefly described|p158||Mesoproterozoic|Of Birksgate Complex.||||||14-OCT-08
19557|Wataru Gneiss|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: within Birksgate Complex, Musgrave Block.||||||07-NOV-08
19557|Wataru Gneiss|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
19557|Wataru Gneiss|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
19557|Wataru Gneiss|50607|5|Briefly described|p1.2, 2.7|||Geological Province: Musgrave Block. Of the Birksgate Complex.||||||
19557|Wataru Gneiss|60662|5|Briefly described|Map Legend|||Mixed layered and massive granulites. Of Birksgate Complex.||||||14-OCT-08
19557|Wataru Gneiss|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Birksgate Complex. Granulite to amphibolite facies granitic gneiss.||||||
19557|Wataru Gneiss|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Granitic gneiss, granulite to amphibolite facies.||||||
19557|Wataru Gneiss|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Granitic gneiss.|
19557|Wataru Gneiss|67536|6|Mentioned|Map Legend|||Musgrave Block.||Of the Birksgate Complex.|||Massive mainly meta-igneous gneiss and granulite, may include charnockite/migmatite alteration of layered granulite; weakly to moderately magnetic.|02-APR-14
19557|Wataru Gneiss|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Granitic gneiss.|
19557|Wataru Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granulite|
19557|Wataru Gneiss|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Gneiss, granulitic, with hornblende, biotite, orthopyroxene, clinopyroxene|
19557|Wataru Gneiss|73090|5|Briefly described|Appendix.|Mesoproterozoic|Mesoproterozoic||||||Gneiss, granulitic, with hornblende, biotite, orthopyroxene, clinopyroxene.|
19609|Wattie Group|14019|4|Described|p14, 29|||Siliclastic sucession with subordinate carbonates. Unconformably overlies Limbunya Group; unconformably overlain by Auvergne Group. Max. thickness: 450m. Geological Province: Victoria Basin. Possibly correlated with Nathan Group.||||||
19609|Wattie Group|23216|6|Mentioned|Fig3p5||Mesoproterozoic|||||||
19609|Wattie Group|23809|5|Briefly described|p47 Fig. 42|||Correlates with the Nathan Group (McArthur Basin).  Geological Province: Victoria Basin.||||||
19609|Wattie Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Victoria Basin.||||||
19609|Wattie Group|24297|3|Fully described|p4|Proterozoic|Proterozoic|Maximum thickness: 450m.  Geological Province: Victoria Basin.   See also p5 Tb. 2.||||||
19609|Wattie Group|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Unconformably overlies the Limbunya Group (Birrindudu Basin); conformably overlain by Timber Creek Formation (Bullita Group). Geological Province: Victoria Basin.||||||
19609|Wattie Group|24442|5|Briefly described|p50 Fig. 1|||Divided into 7 units.  Geological Province: Victoria Basin.||||||
19609|Wattie Group|28255|3|Fully described|p31, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Comprises seven formations/units. Unconformably overlies Limbunya Group; conformably overlain by Timber Creek Formation of the Bullita Group. Max. thickness: 400m.||||||18-DEC-06
19609|Wattie Group|29809|6|Mentioned|p418|||||||||
19609|Wattie Group|30003|4|Described|p8, p12|||Characteristic feature of this group is the presence of 10-20% of white graines, clearly visible in hand specimens - composed of microcline and plagioclase crystals, chert, claystone and other rock fragments, and clay aggregates.||||||19-APR-05
19609|Wattie Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
19609|Wattie Group|32172|4|Described|p9|||Carpentarian or Adelaidean. Table 1||||||
19609|Wattie Group|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean (per legend).||||||17-NOV-04
19609|Wattie Group|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||02-DEC-04
19609|Wattie Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|32660|4|Described|Table 6|||||||||
19609|Wattie Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Sandstone, siltstone, minor dolomite.||||||02-DEC-04
19609|Wattie Group|32701|4|Described|Table 1|||Adelaidean. See p8.||||||18-DEC-06
19609|Wattie Group|32728|6|Mentioned|p16|||||||||
19609|Wattie Group|33374|6|Mentioned|p6|||||||||
19609|Wattie Group|33375|5|Briefly described|p7-8|Adelaidean|Adelaidean|See also Table 1 p8-9.||||||26-APR-05
19609|Wattie Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|33377|5|Briefly described|Table 2|||||||||
19609|Wattie Group|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||27-APR-05
19609|Wattie Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19609|Wattie Group|37462|4|Described|Table 4.VI|||||||||
19609|Wattie Group|38157|6|Mentioned|p284|||||||||
19609|Wattie Group|42012|6|Mentioned|p13|||||||||
19609|Wattie Group|45112|3|Fully described|p18|||p18-19.||||||18-DEC-06
19609|Wattie Group|45140|6|Mentioned|p13, Appx.p19|||Victoria River region.||||Unconformably overlies Limbunya Group.||
19609|Wattie Group|46864|6|Mentioned|Fig.4|||||||||
19609|Wattie Group|48938|4|Described|p21|||||||||
19609|Wattie Group|48943|2|Defined|p39|Adelaidean|Adelaidean|||||||
19609|Wattie Group|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Undifferentiated micaceous siltstone, sandstone, minor dolostone.||||||
19609|Wattie Group|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes seven named units.  Consists of siltstone, sandstone, dolostone.    Geological Province: Victoria Basin.||||||24-NOV-04
19609|Wattie Group|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mainly dolostone, sandstone and siltstone. Unconformably overlies Limbunya Group. Overlain unconfromably by Bullita Group. Geological Province: Victoria Basin.||||||11-JAN-05
19609|Wattie Group|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Bullita Group. Age: 1610-1570Ma. Undifferentiated micaceous siltstone, sandstone and minor dolostone. Geological Province: Victoria Basin.||||||07-NOV-08
19609|Wattie Group|60685|4|Described|p4|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, dolostone. Unconformably overlies Limbunya Group; conformable below Bullita Group. Age: 1.61-1.57Ga. Max. Thickness: 450m. Geological Province: Victoria Basin.||||||07-NOV-08
19609|Wattie Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Victoria River and Birrindudu Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
19609|Wattie Group|65331|5|Briefly described|Map legend + overview geology map legend|Mesoproterozic|Mesoproterozic|Of Victoria Basin. Micaceous siltstone, sandstone, minor dolostone||||||
19609|Wattie Group|65342|5|Briefly described|pp10-11.|||Victoria Basin.|||Includes Wickham, Burtawurta, Mount Sanford and Gibbie Formations; Hughie, Neave and Seale Sandstones.|Is overlain by Bullita Group.|Mainly a siliciclastic succession with minor carbonate intervals.|
19609|Wattie Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Wickham, Burtawurta, Mount Sanford and Gibbie Formations; Hughie, Neave and Seale Sandstones.|Unconformably overlies Limbunya Group. Is unconformably overlain by Bullita Group.||
19609|Wattie Group|68733|5|Briefly described|p177-179, p181 Fig.3, p184, p185 Tb.4|||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).|||Includes Seale, Neave, Hughie Sandstones; Gibbie, Mount Sanford, Burtawurta, Wickham Formations.|||06-DEC-17
19609|Wattie Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|Southern Birrindudu Basin.|||||Includes stromatolitic carbonate rocks and sandstone deposited in sag basins.|12-JUL-16
19609|Wattie Group|69432|4|Described|p17:1-3, 9, 13, 15|||Birrindudu Basin. The base of this unit was selected (by Dunster et al., 2000 and Cutovinos et al., 2002) as the break between the Birrindudu and Victoria Basins. This study places that boundary at the base of the Auvergne Group. A mostly recessive, siliciclastic succession with subordinate carbonate rocks. Age is poorly constrained. Total thickness over 450m, thickening to the E and N. Is gently folded into broad domes, anticlines and synclines 10-50km across. Exploration target for base metals. May have been the source of oil in Timber Creek Formation.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain unconformably by Bullita Group.|Siliciclastic, with subordinate carbonate, rocks.|12-JUL-16
19609|Wattie Group|69441|6|Mentioned|p26:1|||The unconformity at the base of this unit used to mark the separation between the Birrindudu and overlying Victoria Basins (Dunster et al., 2000; Cutovinos et al., 2002). This study relocates the boundary between the Tijunna and Auvergne Groups.||||||12-JUL-16
19609|Wattie Group|69445|5|Briefly described|p30:4|Proterozoic|Proterozoic|Victoria River region, Birrindudu Basin.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
19609|Wattie Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p51|Paleoproterozoic|Paleoproterozoic||||Includes Wickham Formation, Burtawurta Formation, Hughie Sandstone, Mount Sanford Formation, Neave Sandstone, Gibble Formation, Seale Sandstone|Unconformably overlies Limbunya Group, unconformably overlain by Bullita Group||
19609|Wattie Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].|||||Micaceous siltstone, sandstone and minor dolostone.|18-JUL-16
19609|Wattie Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sandford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation.|Unconformably overlies Limbunya Group. Is unconformably overlain by Bullita Group, Auvergne Group.|Micaceous siltstone, sandstone, minor dolostone.|
19609|Wattie Group|70848|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Victoria Basin.|||Wickham Formation.|||
19609|Wattie Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain unconformably by Bullita Group.|Sandstone, siltstone, claystone, chert, dolostone, conglomerate.|
19609|Wattie Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wickham, Burtawurta, Mount Sanford, Gibbie Formations; Hughie, Neave, Seale Sandstones.|Unconformably overlies Limbunya Group. Is overlain by Timber Creek Formation (Bullita Group).|Sandstone, siltstone, claystone, dolostone, chert, conglomerate.|
19609|Wattie Group|70968|5|Briefly described|p6, p130, p132|||Birrindudu Basin.||||Is overlain unconformably by Roper Group. Equivalent of the Nathan Group.||
19609|Wattie Group|71059|5|Briefly described|p7|||Birrindudu Basin.||||Is overlain unconformably by Roper Group. Equivalent to Nathan Group (McArthur Basin).||
19609|Wattie Group|71169|5|Briefly described|p71|Calymmian|Calymmian|North Australian Craton.|c. 1550-1400 Ma|||||
19609|Wattie Group|71302|5|Briefly described|p1-3,6,15,22,72-74||Paleoproterozoic|Of Birindudu Basin.|||Includes Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sanford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation.|Overlain by Bullita Group. Underlain by Limbunya Group.||
19609|Wattie Group|71374|6|Mentioned|p2|||Birrindudu Basin.||||||
19609|Wattie Group|72373|5|Briefly described|p2,36,39|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin. Broadly equivalent to Favenc package, Nathan, Mount Rigg, Balma groups and Karns Dolostone (McArthur Basin) and Namerinni Group (Tomkinson province).||||||
19609|Wattie Group|72718|6|Mentioned|p7, p9|||Birrindudu Basin. Equivalent to the Favenc package.|||Seale Sandstone, Gibbie Formation, Neave Sandstone, Mount Sanford Formation, Hughie Sandstone, Burtawurta Formation, Wickham Formation|Unconformably[?] underlain by Killaloc Formation (Limbunya Group). Overlain by Timber Creek Formation (Bullita Group).||
19609|Wattie Group|73083|6|Mentioned|p30||||||Wickham Formation|Unconformably underlain by Limbunya Group.||
19643|Weaber Group|13194|4|Described|p388 Tb. 4-16, p382 fig 4-59|Upper Carboniferous|Tournaisian|600-2400m thick upward coarsening and shallowing sequence.||||||
19643|Weaber Group|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
19643|Weaber Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin.  Max. thickness: 2400 m.||||||22-DEC-06
19643|Weaber Group|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Sandstone, limestone, and minor conglomerate, shale and siltstone.  Geological Province: Bonaparte Basin.||||||
19643|Weaber Group|24569|5|Briefly described|p248 Fig. 3|Namurian|Visean|Includes the Point Spring Sandstone, Tanmurra and Milligans Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
19643|Weaber Group|32701|6|Mentioned|p17|||Refers Traves (1955)||||||
19643|Weaber Group|40993|6|Mentioned|Fig.1|||||||||
19643|Weaber Group|41459|6|Mentioned|Fig.2|||||||||
19643|Weaber Group|41532|4|Described|p292|||||||||
19643|Weaber Group|41598|6|Mentioned|p412|||||||||
19643|Weaber Group|41731|6|Mentioned|Fig.3|||||||||
19643|Weaber Group|41864|4|Described|p123|||||||||
19643|Weaber Group|41865|6|Mentioned|Map legend|Westphalian|late Tournaisian|||||||
19643|Weaber Group|42055|4|Described|Fig.1 P52|||||||||
19643|Weaber Group|42056|4|Described|p96|||||||||
19643|Weaber Group|42442|3|Fully described|p11|||||||||
19643|Weaber Group|42933|5|Briefly described|Fig.94 p258|||||||||
19643|Weaber Group|43236|6|Mentioned|p14,Fig.13.|Namurian|Visean|||||||
19643|Weaber Group|43661|6|Mentioned|Fig.3|||||||||
19643|Weaber Group|44965|14|Not recorded|Not recorded|||||||||
19643|Weaber Group|45038|14|Not recorded|p.27,30,78,86,94||Permian|Perm?||||||
19643|Weaber Group|48938|6|Mentioned|p75|||Refers Traves.||||||
19643|Weaber Group|60006|5|Briefly described|Map Legend|Namurian|Visean|Geological Province: Bonaparte Basin. Sandstone, siltstone, conglomerate, shale, limestone||||||22-JUL-04
19643|Weaber Group|60364|5|Briefly described|p184|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
19643|Weaber Group|60386|6|Mentioned|p297|Carboniferous|Carboniferous|Roebuck/Canning Basin. Deltaic - nearshore - shelf. Post Alice Springs Orogeny.||||||
19643|Weaber Group|60682|4|Described|piii|Carboniferous|Carboniferous|Unconformably overlies Langfield Group. Unconformably overlain by Kulshill Group. Max. thickness: >2400m. Geological Province: Bonaparte Basin. Shoreface, deltaic and fluvial deposits.||||||19-DEC-06
19643|Weaber Group|61542|1|Redefined|p276, p277 Fig. 2|Early Carboniferous|Early Carboniferous|Of Mory and Beere (1988).Originally incl: Milligans+Waggon Creek Fms, Utting Calcarenite, Burvill+Tanmurra Fms+Point Spring Sst. Here revised to exclude Pt Spring Sst; Waggon Ck Fm is relegated to a facies association (mbr). New subdivisions introduced.||||||07-FEB-11
19643|Weaber Group|62837|5|Briefly described|Stratigraphic columns|Namurian|Tournaisian|Includes Milligans and Tanmurra Formations and Point Spring Sandstone.  Age: <345-~311Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
19643|Weaber Group|64580|4|Described|map legend|Pennsylvanian|Mississippian|Undivided; siltstone, shale, sandstone, conglomerate; subordinate carbonate; includes TANMURRA, MILLIGANS, WAGGON CREEK and BURVILL FORMATIONS, UTTING CALCARENITE, and POINT SPRING SANDSTONE.||||||09-DEC-08
19643|Weaber Group|64630|5|Briefly described|p31 Fig.2|Serpukhovian|Visean|Province: Bonaparte Basin. Unconformably underlies the Wadeye Group. Palynology age: G. maculosa to S. ybertii.||||||18-JAN-10
19643|Weaber Group|64689|5|Briefly described|p16|Carboniferous|Carboniferous||||Includes the Milligans Formation.|||
19643|Weaber Group|64694|5|Briefly described|p231, p232, p233, p239, p249|Namurian|Tournaisian|Bonaparte Basin.||Unit in Weaber Group.|Includes Waggon Creek, Lower and Upper Milligans, Burvill, Tanmurra Formations; Utting Calcarenite; Point Spring Sandstone.|Overlies the Langfield Group unconformably.||
19643|Weaber Group|65331|5|Briefly described|Map legend + overview geology map legend|Bashkirian|Visean|Of Bonaparte Basin. Includes Point Spring Sandstone, Burvill Formation, Milligans Formation. Age shown as Visean to Namurian. Sandstone, siltstone, conglomerate, shale, limestone||||||
19643|Weaber Group|66498|6|Mentioned|p48|||Bonaparte Basin, WA.|||Utting Calcarenite.|||
19643|Weaber Group|67354|6|Mentioned|p73. ||||||Includes Wadeye Sub-Group and Sunbird Formation.|||
19643|Weaber Group|69099|4|Described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra, Milligans, Waggon Creek and Burvill Formations, Utting Calcarenite, and Point Spring Sandstone||siltstone, shale, sandstone, conglomerate; subordinate carbonate;|
19643|Weaber Group|69165|4|Described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra Formation, Milligans Formation, Burvill Formation, Waggon Creek Formation, Utting Calc-arenite, Point Spring Sandstone||Undivided; siltstone, shale, sandstone and conglomerate; subordinate carbonate.|
19643|Weaber Group|69422|6|Mentioned|p7:2 Fig.7.2|Carboniferous|Carboniferous|Bonaparte Basin.||||||12-JUL-16
19643|Weaber Group|69452|4|Described|p36:4, 7, 9, 11-17|Early Carboniferous|Early Carboniferous|Traves (1955); Gorter et al. (2005). Petrel Sub-basin, Bonaparte Basin. Onshore and offshore. c.2400m thick. Originally included Point Spring Sandstone as the topmost unit; since assigned to the Wadeye Group by Gorter et al. (2005). Latest Tournaisian to early Serpukhovian age.|||Milligans, Yow Creek, Burvill, Tanmurra, Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Ningbing Group disconformably and Langfield Group unconformably. Is overlain unconformably by the Wadeye Group.|A complex succession of clastic and carbonate sedimentary rocks, separated by several unconformities.|12-JUL-16
19643|Weaber Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian||||Includes Tanmurra Formation, Milligans Formatrion, Waggon Creek Formation, Utting Calcarenite and Point Springs Sandstone.||Undivided; siltstone, shale, sandstone, conglomerate; subordinate carbonate|
19643|Weaber Group|69653|6|Mentioned|p10, 14-15|Carboniferous|Carboniferous|Petrel Sub-basin.|||Milligans, Yow Creek, Tanmurra, Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Langfield Group. Is overlain by Kulshill Group.||
19643|Weaber Group|69673|6|Mentioned|p166 fig 136, p171, p179|Carboniferous|Carboniferous|Up to 2400m thick.|||Includes Milligans Formation, Yow Creek Formation, Utting Calcarenite, Kingfisher Shale, Tanmurra Formation, Sandbar Sandstone, Sunbird Formation|Overlain by Kinmore Group, Wadeye Group, unconformably overlies Langfield Group||
19643|Weaber Group|70061|5|Briefly described|Petrel Sub-basin; Fig.3|Serpukhovian|Tournaisian|See also Regional geology: Fig.8, p8. Intraformational seal.|||Milligans, Yow Creek, Tanmurra and Sunbird Formations; Utting Calcarenite; Kingfisher Shale; Sandbar Sandstone.|Overlies Bonaparte Formation. Is overlain by Wadeye Group.||12-JUL-16
19643|Weaber Group|70064|5|Briefly described|Regional Fig. 6|Bashkirian|Tournaisian|Caswell-Barcoo Sub-basins, Browse Basin.||||Is overlain by Kulshill Group.||12-JUL-16
19643|Weaber Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Pennsylvanian|Tournaisian||298-350 Ma||||Siltstone, shale, sandstone, conglomerate; subordinate carbonate|
19643|Weaber Group|70206|5|Briefly described|Map Legend, cross-sect.|Carboniferous|Carboniferous|Bonaparte Basin.|||Includes Point Spring Sandstone, Burvill Formation, Milligans Formation, Waggon Creek Formation, Tanmurra Formation.|Unconformably overlies Langfield Group.||
19643|Weaber Group|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Bonaparte Basin.||||||
19643|Weaber Group|70851|6|Mentioned|p17|||||||||
19643|Weaber Group|71146|5|Briefly described|p6, p34,  p43 fig 33|Visean|Tournaisian|Bonaparte Basin. Believed to be partially equivalent to the Williambury Formation.||||Unconformably overlies the Bonaparte Formation and the Langfield Group. Unconformably overlain by the Wadeye Group.|Mudstone, sandstone and carbonate.|
19643|Weaber Group|71267|4|Described|GEOL_LUT_CSV files|Pennsylvanian|Tournaisian|Of Burt Range Shelf; Carlton Shelf, Southern Bonaparte Basin. Events: Gondwana breakup-northern NW Shelf (320-138 Ma); Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|350-298.9 Ma (biostrat)||Includes Milligans Formation, Burvill Formation.||Quartz sandstone, siltstone, shale, minor limestone and conglomerate. Shoreface, deltaic and fluvial deposits|
19643|Weaber Group|72034|5|Briefly described|500k_interpgeop16_lut|Pennsylvanian|Tournaisian|Burt Range Shelf; Carlton Shelf, Southern Bonaparte Basin.  Age from biostratigraphy.|||||Siltstone, shale, sandstone, conglomerate; subordinate carbonate.|
19643|Weaber Group|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.|||Sunbird Formation, Sandbar Sandstone, Tanmurra Formation, Kingfisher Shale, Burvill Formation, Utting Calcarenite, Yow Creek Formation, Milligans Formation.|||
19668|Weedarra Shale|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Overlying unit: Carrandibby Formation. Underlying unit: Thambrong Formation. Of the Lyons Group.||||||
19668|Weedarra Shale|32648|6|Mentioned|p32|||Equiv. Carrandibby Fm.||||||
19668|Weedarra Shale|36890|6|Mentioned|p279|||||||||
19668|Weedarra Shale|37295|6|Mentioned|Table 2|||||||||
19668|Weedarra Shale|41271|6|Mentioned|p65|||||||||
19668|Weedarra Shale|44344|14|Not recorded|p.6,9-10,24||Sakmarian|Sakmarian; topmost fm. of Lyons Group. (G50-1). opp.4, map.||||||
19668|Weedarra Shale|44345|14|Not recorded|map legend||Sakmarian|Sakmarian.||||||
19668|Weedarra Shale|44532|4|Described|p.6,15,16, map|||Shale aquifer. (G50-5).||||||
19668|Weedarra Shale|44533|5|Briefly described|map legend||Sakmarian|Sakmarian.||||||
19668|Weedarra Shale|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group.||||||01-JUN-06
19668|Weedarra Shale|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
19674|Weeli Wolli Formation|22689|6|Mentioned|Fig. 1 p138|||Of Hamersley Group.||||||
19674|Weeli Wolli Formation|23045|5|Briefly described|289|||Parent Hamersley Group||||||
19674|Weeli Wolli Formation|23046|6|Mentioned|171|||||||||
19674|Weeli Wolli Formation|23126|5|Briefly described|p383 Fig.3|||||||||
19674|Weeli Wolli Formation|23280|5|Briefly described|p1085,Table1p1085||Siderian|Max Age: 2449 (+/-) 3 Ma.||||||
19674|Weeli Wolli Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
19674|Weeli Wolli Formation|23536|5|Briefly described|Fig 2 p 429|||||||||
19674|Weeli Wolli Formation|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Overlying unit Woongarra Rhyolite. Underlying unit Brockman Iron Formation.||||||
19674|Weeli Wolli Formation|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
19674|Weeli Wolli Formation|24041|5|Briefly described|p493|||||||||
19674|Weeli Wolli Formation|24231|5|Briefly described|p186 Fig.2|||Geological Province: Hamersley Basin.||||||
19674|Weeli Wolli Formation|24541|3|Fully described|p2, p11 Tb.2, p57|Paleoproterozoic|Neoarchean|Overlies the Brockman Iron Formation. Of the Hamersley Group. Maximum Thickness: 600m. Geological Province: Hamersley Basin.||||||07-NOV-08
19674|Weeli Wolli Formation|24543|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group (Mount Bruce Supergroup).  Thinly laminated jaspilite; locally brecciated.  Age: c.2490Ma.||||||07-NOV-08
19674|Weeli Wolli Formation|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Hamersley Group. Overlies Brockman Iron Formation. Overlain by Woongarra Rhyolite. Basalt and banded iron-formation. Age: 2449 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
19674|Weeli Wolli Formation|24573|6|Mentioned|p672 Fig.3|||Geological Province: Pilbara Craton||||||
19674|Weeli Wolli Formation|29629|5|Briefly described|p899|||||||||
19674|Weeli Wolli Formation|29716|4|Described|Table 1|||||||||
19674|Weeli Wolli Formation|29717|6|Mentioned|p1155|||||||||
19674|Weeli Wolli Formation|30488|6|Mentioned|p82|||Stratigraphy. See also geochemical data P91||||||
19674|Weeli Wolli Formation|31021|6|Mentioned|Fig. 1|||||||||
19674|Weeli Wolli Formation|31154|6|Mentioned|p71|||||||||
19674|Weeli Wolli Formation|31311|6|Mentioned|p62|||re age dates||||||
19674|Weeli Wolli Formation|31671|5|Briefly described|p12|||||||||
19674|Weeli Wolli Formation|31819|6|Mentioned|p86|||||||||
19674|Weeli Wolli Formation|31828|6|Mentioned|p40|||Stratigraphic table||||||
19674|Weeli Wolli Formation|33538|6|Mentioned|p291|||||||||
19674|Weeli Wolli Formation|33540|6|Mentioned|Fig.2|||||||||
19674|Weeli Wolli Formation|33542|6|Mentioned|p412|||||||||
19674|Weeli Wolli Formation|33544|1|Redefined|p89|Proterozoic|Proterozoic|See also pp90 - 92||||||18-SEP-15
19674|Weeli Wolli Formation|33687|5|Briefly described|p918|||Also p921 re mineralization||||||18-SEP-15
19674|Weeli Wolli Formation|34066|4|Described|p6|||L.Prot.||||||
19674|Weeli Wolli Formation|34135|5|Briefly described|Table 1|||See also Table 2, pp13,17. Lower Proterozoic||||||18-SEP-15
19674|Weeli Wolli Formation|35036|6|Mentioned|p295|||||||||
19674|Weeli Wolli Formation|35299|6|Mentioned|Fig.1|||||||||
19674|Weeli Wolli Formation|35976|6|Mentioned|p110|||See also Fig.39.||||||
19674|Weeli Wolli Formation|36004|4|Described|p1089|||Discussion re sedimentology.||||||
19674|Weeli Wolli Formation|36247|6|Mentioned|Fig.2|||||||||
19674|Weeli Wolli Formation|36551|6|Mentioned|Table 23|||||||||
19674|Weeli Wolli Formation|36882|4|Described|p133|||||||||
19674|Weeli Wolli Formation|37297|6|Mentioned|p96|||||||||
19674|Weeli Wolli Formation|37460|6|Mentioned|Fig.3.4|||||||||
19674|Weeli Wolli Formation|37704|6|Mentioned|Fig.1|||||||||
19674|Weeli Wolli Formation|37708|6|Mentioned|Fig.1|||||||||
19674|Weeli Wolli Formation|38321|6|Mentioned|Table 1|||||||||
19674|Weeli Wolli Formation|38790|6|Mentioned|p161|||||||||
19674|Weeli Wolli Formation|39200|6|Mentioned|Fig.4|||||||||
19674|Weeli Wolli Formation|39210|5|Briefly described|Table 1|||||||||
19674|Weeli Wolli Formation|39697|5|Briefly described|p126|||See also p171.||||||18-SEP-15
19674|Weeli Wolli Formation|39952|5|Briefly described|p289|||||||||
19674|Weeli Wolli Formation|40109|5|Briefly described|p323|||||||||
19674|Weeli Wolli Formation|41358|6|Mentioned|Fig.2|||||||||
19674|Weeli Wolli Formation|41622|6|Mentioned|Fig.2|||||||||
19674|Weeli Wolli Formation|41847|5|Briefly described|p104|||||||||
19674|Weeli Wolli Formation|42112|4|Described|p10|||||||||
19674|Weeli Wolli Formation|42148|6|Mentioned|Table 1 P687|||||||||
19674|Weeli Wolli Formation|42260|6|Mentioned|p11|||||||||
19674|Weeli Wolli Formation|42471|4|Described|p8|||||||||
19674|Weeli Wolli Formation|42472|5|Briefly described|Map legend|||||||||
19674|Weeli Wolli Formation|42495|4|Described|p4-23|||||||||
19674|Weeli Wolli Formation|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
19674|Weeli Wolli Formation|42704|5|Briefly described|Plate 2E|Proterozoic|Archean|Of the Hamersley Group. Interlayered BIF, often jaspilitic and metadolerite sills.||||||07-NOV-08
19674|Weeli Wolli Formation|42743|5|Briefly described|map legend|Proterozoic||||||||
19674|Weeli Wolli Formation|42744|5|Briefly described|p5|||||||||
19674|Weeli Wolli Formation|43119|5|Briefly described|p11|||of Hamersley Group||||||
19674|Weeli Wolli Formation|43210|5|Briefly described|Table 1p3,p5.||Paleoproterozoic|of Hamersley Group.||||||07-NOV-08
19674|Weeli Wolli Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Hamersley Group.||||||
19674|Weeli Wolli Formation|43290|5|Briefly described|p7||Proterozoic|of Hamersley Group. Unit listed as 600m thick and 5-10m thick.||||||
19674|Weeli Wolli Formation|43595|6|Mentioned|Fig.2-49,p220|||||||||
19674|Weeli Wolli Formation|44152|5|Briefly described|p178-180, p182, p185-188, p191|||Detailed comparison of this with similar BIF units of Hamersley Group on p185. The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Hamersley Group.||Overlies Yandicoogina Shale Member (Brockman Iron Formation). Is overlain by Woongarra Volcanics.|BIF, shale.|
19674|Weeli Wolli Formation|44438|14|Not recorded|map legend||Paleoproterozoic|Formation of Hamersley Group of Mt. Bruce Supergroup. L.Proterozoic.||||||07-NOV-08
19674|Weeli Wolli Formation|44477|4|Described|p.11, Table 1||Proterozoic|SF/50-6.||||||
19674|Weeli Wolli Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
19674|Weeli Wolli Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
19674|Weeli Wolli Formation|44501|4|Described|p.6,7,12,20,tb4, map||Paleoproterozoic|(ref. to MacLeod et al 1963). (F/50-7). Lower Proterozic.||||||07-NOV-08
19674|Weeli Wolli Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19674|Weeli Wolli Formation|44503|2|Defined|p.5,9,12,Tb.2, map|||Roy Hill Sheet. (F50-12).||||||
19674|Weeli Wolli Formation|44504|14|Not recorded|map legend||Proterozoic|||||||
19674|Weeli Wolli Formation|44692|4|Described|p.7,13,Tb.1, map|||(F50-11). See also p.15,16, for more details.||||||
19674|Weeli Wolli Formation|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
19674|Weeli Wolli Formation|50227|5|Briefly described|p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group.  Geological Province: Hamersley Province.  See also p447 Fig. 3.||||||07-FEB-11
19674|Weeli Wolli Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
19674|Weeli Wolli Formation|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersly Group. Overlian by Woongarra Volcanics, underlain by Brockman Iron Formation.||||||
19674|Weeli Wolli Formation|60706|5|Briefly described|p623 Fig.2|||Of the Hamersley Group. Geological Province: Hamersley Basin. Ages: 2449+/-3 Ma (Barley et al., 1997), 2450+/-3 Ma age of (overlying) Woongarra Rhyolite from joint regression of data of Barley et al.( 1997). Max age: 2451Ma - interpolated.||||||06-OCT-15
19674|Weeli Wolli Formation|61268|5|Briefly described|p81 Tb.1, p84|||Of the Hamersley Group. Thinly laminated jaspelite, siltstone, and shale. See also p80 Fig.2, p83 Fig.4.||||||
19674|Weeli Wolli Formation|62129|3|Fully described|p10, p19|Archaean|Archaean|Of Hamersley Group. Conformably overlies Brockman Iron Formation, conformably overlain by Woongarra Rhyolite. Thickness: 500m. Geological Province: Hamersley Basin. Consists of jaspilitic, iron-formation, together with shale and chert.||||||07-FEB-11
19674|Weeli Wolli Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Banded iron-formation (commonly jasperilitic), pelite, and numerous metadolerite sills.||||||23-MAR-09
19674|Weeli Wolli Formation|63153|6|Mentioned|p1362 Fig.3, p1363 Fig.4.|||||Unit in Hamersley Group.||Overlies Brockman Iron Formation. Is overlain by Woongarra Volcanics.||
19674|Weeli Wolli Formation|63236|6|Mentioned|Map legend|||Some of this formation is included in the mapping of Brockman Iron Formation.||||||17-SEP-07
19674|Weeli Wolli Formation|63372|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Hamersley Basin. Age: 2449Ma. Banded iron formation (commonly jaspilitic), mudstone, siltstone and numerous dolerite sills. Underlies: Woongarra Rhyolite. Overlies: Brockman Iron Formation.||||||07-NOV-08
19674|Weeli Wolli Formation|63432|5|Briefly described|p735, p736 Fig. 3|||Of the Hamersley Group. Geological Province: Hamersley Province. Deeply weathered dolerite sills and shales / flaggy-shaley BIF. See also p743, p751.||||||07-FEB-11
19674|Weeli Wolli Formation|64384|5|Briefly described|p35 Tb. 6, p37|||Of the Hamersley Group.Overlies Brockman Iron Formation. Geological province: Hamersley Basin. Sequence of interbedded BIF (often jaspilitic, up to 10m thick), chert, shale, dolerite sills which has been intruded by several metadolerite sills.||||||07-FEB-11
19674|Weeli Wolli Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Upper Hamersley Group. Banded iron-formation (often jaspilitic), mudstone, siltstone, and numerous dolerite sills; metamorphosed.||||||09-DEC-08
19674|Weeli Wolli Formation|64688|5|Briefly described|Map legend|||Some of these rocks are included in Brockman Iron Formation in this iron ore geology mapping.||||||
19674|Weeli Wolli Formation|64724|5|Briefly described|p42 Fig. 3|Paleoproterozoic|Paleoproterozoic|Hamersley Basin unit.||Of Hamersley Group.||||02-APR-12
19674|Weeli Wolli Formation|64725|6|Mentioned|p58.|||||Unit in Hamersley Group.||Overlies Brockman Iron-formation. Is overlain by Woongarra Rhyolite.||
19674|Weeli Wolli Formation|65194|5|Briefly described|p109|||Shale, dolerite and BIF.||||||
19674|Weeli Wolli Formation|65683|5|Briefly described|p801 Fig2|||Of Hamersley Group. Underlies Woongarra Volcanics; overlies Yandicoogina Shale Member of Brockman Iron Formation.||||||08-MAR-12
19674|Weeli Wolli Formation|65757|5|Briefly described|p84 Fig.2, p88|||In part banded iron formation. Underlies the Wongarra Rhyolite, overlies the Yandicoogina Member, Brockman Iron Formation. Misspelt as Weeli Wollie Formation p88.||||||
19674|Weeli Wolli Formation|66526|5|Briefly described|p37.|Proterozoic|Proterozoic|Pilbara Province. Dolerite dykes and sills and basalt, with correlative Blackfellow Hill Pyroxenite in Central Gawler Province, produced in the Weeli Wolli Event, ME 1 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.2455 Ma.|||||
19674|Weeli Wolli Formation|66574|6|Mentioned|p914|||Unit in upper Hamersley Group. Intruded by dolerite sills.||||||15-SEP-14
19674|Weeli Wolli Formation|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~2500 Ma estimated from Fig.11.|||||
19674|Weeli Wolli Formation|67025|4|Described|pp318-328.|||Contains iron ore deposits. The natural remanent magnetisation and mean bulk susceptibility of this unit are discussed in this article.||Unit in Hamersley Group.||Conformably overlies Brockman Iron Formation. Is overlain conformably by Woongarra Volcanics.||
19674|Weeli Wolli Formation|67056|5|Briefly described|p419 Fig.2, p423. |||A possible source for a BIF jasper-rich type pebble conglomerate with occasional ore pebbles, which occurs in the Wyloo Group.||Unit in Hamersley Group.||Overlies Brockman Iron Formation. Is intruded by extensive dolerite sills. Is overlain by Woongarra Rhyolite.||
19674|Weeli Wolli Formation|67130|6|Mentioned|p8 fig 5, p40 fig 38|||||Hamersley Group||Overlies Brockman Iron Formation, overlain by Woongarra Volcanics|Banded iron formation, dolerite.|
19674|Weeli Wolli Formation|67183|6|Mentioned|p645 Tb.1 |Archean|Archean|Present in the Southern Pilbara.||Hamersley Group||||
19674|Weeli Wolli Formation|67201|5|Briefly described|p32, p34-35, p52-53, p56|||||Hamersley Group||Overlies Joffre Member (Brockman Iron Formation).|BIF-dominated; distinguished by metadolerite sills.|
19674|Weeli Wolli Formation|67721|5|Briefly described|p38 Fig.9|Siderian|Siderian|Approximately 450 m thick.|c. 2449 Ma|Of the Hamersley Group.|||Shaly banded iron formations, banded iron formation, shales, dolerite sills.|
19674|Weeli Wolli Formation|67855|6|Mentioned|p225|||Hamersley Basin.||||overlain by Beasley River Quartzite near Deadman Hill.||
19674|Weeli Wolli Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Of Hamersley Group.||Overlies Brockman Iron Formation. Overlain by Woongarra Rhyolite.|BIF-dominated.|
19674|Weeli Wolli Formation|68280|6|Mentioned|p5, p48, p54|||||Hamersley Group||Overlain by Woongarra Rhyolite, overlies Brockman Iron Formation|Banded iron formation.|
19674|Weeli Wolli Formation|69028|5|Briefly described|Map Legend|Siderian||Hamersley Basin.||Of the Hamersley Group.|||Banded iron-formation (commonly jaspilitic), mudstone, siltstone and numerous dolerite sills; metamorphosed.|18-SEP-15
19674|Weeli Wolli Formation|69080|6|Mentioned|p687|||||Unit in Hamersley Group.||Overlies Brockman Iron Formation. Is overlain by Boolgeeda Iron Formation.||
19674|Weeli Wolli Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Banded iron-formation (often jaspilitic), mudstone, siltstone, and numerous dolerite sills; metamorphosed.|
19674|Weeli Wolli Formation|69185|5|Briefly 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.|||Banded iron-formation (often jaspilitic), mudstone, siltstone, and numerous dolerite sills; metamorphosed|
19674|Weeli Wolli Formation|69538|6|Mentioned|p517 Fig.3, p525 Fig.6, p526, p530|Paleoproterozoic|Paleoproterozoic|See also p532 Tb.3, p534, p557 Fig.32, p579.||Unit in Hamersley Group.||||
19674|Weeli Wolli Formation|69563|6|Mentioned|p691 Fig.1|||||Unit in Hamersley Group.||||
19674|Weeli Wolli Formation|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.||Hamersley Group.||Is overlain by Woongarra Rhyolite.||
19674|Weeli Wolli Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Hamersley Group.||||
19674|Weeli Wolli Formation|69590|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Of Hamersley Basin. Events: Paterson Orogeny; Miles Orogeny.||Unit of Hamersley Group.|||Banded iron-formation (often jaspilitic), mudstone, siltstone, and numerous dolerite sills; metamorphosed|
19674|Weeli Wolli Formation|69739|6|Mentioned|p69-70|||Hamersley Basin.||||||
19674|Weeli Wolli Formation|69745|6|Mentioned|p272-273, 275-277, 281, 284, 287, 290|||Crops out in the Mount Wall Fe deposit area, Hamersley Province.||Hamersley Group.||||
19674|Weeli Wolli Formation|70086|5|Briefly described|p196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Hamersley Group.||Overlain by Woongarra Rhyolite.||
19674|Weeli Wolli Formation|70509|5|Briefly described|p13-14,33|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton.||Unit of Hamersley Group.||Overlain by Woongarra rhyolite. Underlain by Brockman Iron Formation.||
19674|Weeli Wolli Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2451-2450 Ma||||Banded iron formation (commonly jaspilitic), mudstone, siltstone and numerous dolerite sills; metamorphosed.|
19674|Weeli Wolli Formation|70958|6|Mentioned|p16|||Misspelt Welli Welli Formation, Hamersley Group.||||||
19674|Weeli Wolli Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|Oakover Basin.||Hamersley Group||||
19674|Weeli Wolli Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||mudstone, siltstone, dolerite, banded iron formation|
19674|Weeli Wolli Formation|71513|6|Mentioned|p66,|||Pilbara Craton. Interpreted to have been deposited in a back-arc setting.||Hamersley Group|||Dolerite and basalt.|
19674|Weeli Wolli Formation|71808|4|Described|viii-ix, p2, p34, p39-p41|||Hamersley Province. Forms characteristic strike parallel ridges of BIF and syn-sedimentary dolerite and tuffaceous shale. Extensively intruded by unnamed and numerous dolerite sills. A measured section at Woongarra Pool in the western Province comprises a total of 184m of BIF with minor shale and 269m of dolerite in eight sills. Originally the basal part of this unit was included in the Brockman Iron Formation as the now obsolete Coondiner Member. This unit is distinguishable in airphotography. Subdivided into three informal units on the basis of lithology. See also p44-p47, p53, p85, p93, p117, p149, p156, p250.||Hamersley Group||Overlies the Yandicoogina Shale Member and Joffre Member. Overlain by the Woongarra Rhyolite.|Banded iron formation,red chert,  dolerite, tuffaceous shale.|
19674|Weeli Wolli Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Hamersley Group, upper|||Banded iron-formation (commonly jaspilitic), mudstone, siltstone, and numerous dolerite sills; metamorphosed.|
19674|Weeli Wolli Formation|72447|6|Mentioned|p240|||||||||
19674|Weeli Wolli Formation|72493|5|Briefly described|p30, 35, 43|||Hamersley Basin.|2445 +/- 5 Ma.|Hamersley Group.||OverliesYandicoogina Shale Member (Brockman Iron Formation). Is overlain by Woongarra Rhyolite.|BIF, dolerite.|
19674|Weeli Wolli Formation|72570|6|Mentioned|p3 fig 1|||||Hamersley Group||||
19674|Weeli Wolli Formation|72712|5|Briefly described|p7, p9, p10, p31, p35.|Siderian|Siderian|See also p11 Fig.8, p32 Fig.24, p55. This formation is well exposed in a creek section along the Beasley River at Woongarra Pool.|c. 2460 Ma to c. 2449 Ma.|Hamersley Group||Shown as overlying Brockman Iron Formation and underlying Woongarra Rhyolite. Intruded by dolerite sills.|Includes BIF and chert with jaspillite clasts showing weak hematite replacement of laminae.|
19674|Weeli Wolli Formation|72758|5|Briefly described|p15 Tb.1, p23, p25, p28.|||Formation up to 480m thick.||Hamersley Group||Conformably overlies Brockman Iron Formation and underlies Woongarra Volcanics. Intruded by dolerite sills.|BIF interlayered with thick beds of shale and numerous dolerite sills. Includes dark, red-brown rock with 2-5 mm layers of hematite-rich chert, and beds of red or white laminated chert.|
19674|Weeli Wolli Formation|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Hamersley Group||Overlies the Brockman Iron Formation, underlies the Woongarra Rhyolite.|Dolerite sills, banded iron formation, minor shale and Fe-chert.|
19674|Weeli Wolli Formation|73290|6|Mentioned|p784|||Hamersley Province.||||||
19674|Weeli Wolli Formation|73538|6|Mentioned|p3-4|Siderian|Siderian|Age of 2450 +/- 3 Ma reported by Trendall et al. (2004). [Probably misspelt as Weeli Wooli Formation on p3].|2450 +/- 3 Ma|Hamersley Group||Underlain by Yandicoogina Shale Member of the Brockman Iron Formation. Overlain by Woongarra Rhyolite.|Includes mixed iron formation and mafic volcanics.|
19674|Weeli Wolli Formation|73574|6|Mentioned|p770|||||||||
19735|Wenmillia Formation|30948|6|Mentioned|Map legend|Precambrian|Precambrian|Precambrian undetermined||||||
19735|Wenmillia Formation|32649|4|Described|p8|||See also Table 1||||||
19735|Wenmillia Formation|36293|2|Defined|p74|Proterozoic|Proterozoic|||||||
19735|Wenmillia Formation|36551|6|Mentioned|p141|||||||||
19735|Wenmillia Formation|36872|4|Described|p72|||||||||
19735|Wenmillia Formation|37460|4|Described|p177|||||||||
19735|Wenmillia Formation|40089|6|Mentioned|p12|||||||||
19735|Wenmillia Formation|40340|6|Mentioned|p7|||||||||
19735|Wenmillia Formation|41341|6|Mentioned|p8|||||||||
19735|Wenmillia Formation|44138|5|Briefly described|p264 Fig.3-54, p265, p272|||Deformed, low-grade metasedimentary rocks. 300m thick. Near Darling Fault converted to phyllonite.|||||Siltstone, shale and basalt.|
19735|Wenmillia Formation|64722|6|Mentioned|Fig. 9 p. 19|Proterozoic|Proterozoic|Yilgarn margin.||||||11-APR-12
19785|West Kimberley Lamproite|40811|5|Briefly described|p317|||Misspelling of West Kimberly? [unlikely to be misspelling - CB 12-OCT-94]||||||
19792|West Warrery Satellite Granodiorite|38242|6|Mentioned|Fig.2|||||||||
19807|Western Creek Gabbro|42112|5|Briefly described|Table 2 p4|||||||||11-DEC-08
19807|Western Creek Gabbro|43210|6|Mentioned|p3|||||||||
19862|Wharton Sandstone|38632|6|Mentioned|p21|||||||||
19881|Whitby Sandstone|30939|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19881|Whitby Sandstone|33044|6|Mentioned|Map 3|||Shown on map 3 as part of Cardup Gp.||||||
19881|Whitby Sandstone|36293|2|Defined|p71|Proterozoic|Proterozoic|Type section in Mundijong railway cutting. Thickness: up to ~40m.||Of Cardup Group.||Unconformable on Archean rocks, overlain conformably by Neerigen Formation|orthoquartzite, boulder conglomerate, silty sandstone|19-DEC-13
19881|Whitby Sandstone|36872|4|Described|p77|||||||||
19881|Whitby Sandstone|37460|6|Mentioned|p178|||||||||
19889|White Flag Formation|22534|6|Mentioned|p9|||||||||
19889|White Flag Formation|23786|5|Briefly described|p3|||Of the Black Flag Beds?  Geological Province: Yilgarn Craton.||||||
19889|White Flag Formation|24139|5|Briefly described|p238|Archean|Archean|Geological Province: Coolgardie Domain.  Of the Black Flag Beds.  Age: 2681 +/- 5Ma.||||||07-NOV-08
19889|White Flag Formation|24196|5|Briefly described|p47 Fig.5|Archean|Archean|Age: 2813 +/- 3 Ma. Unconformably overlies the Black Flag Formation. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||07-NOV-08
19889|White Flag Formation|42221|6|Mentioned|Table 1 P6|||||||||
19889|White Flag Formation|42696|6|Mentioned|Plate 1B|||||||||
19889|White Flag Formation|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
19889|White Flag Formation|42892|5|Briefly described|p52, Table 5|||||||||
19889|White Flag Formation|43162|6|Mentioned|5|||||||||
19889|White Flag Formation|43496|6|Mentioned|9|||Age: 2675+/-6Ma||||||
19889|White Flag Formation|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Of the Black Flag Group. Underlain by Spargoville Formation. Geological Province: Coolgardie Domain, Yilgarn Craton. Felsic vocanic and sedimentary unit.||||||07-FEB-11
19889|White Flag Formation|60627|5|Briefly described|p65 Tb.1|||Of Black Flag Group.||||||
19889|White Flag Formation|63981|6|Mentioned|p91, p93 Fig.3, |Archean|Archean|This name replaced (Hunter 1993) White Flag Series (of Forman 1937).||Unit in Black Flag Group.||||
19889|White Flag Formation|64633|6|Mentioned|p4 Fig.3, p6 Fig.4.|||Kalgoorlie Terrane.|2690 +/- 9 Ma.|Unit in Kalgoorlie Sequence.||||
19889|White Flag Formation|65834|6|Mentioned|p7|||Coolgardie Domain, Kalgoorlie Terrane.||Black Flag Group.||||
19889|White Flag Formation|66880|6|Mentioned|p8 Fig.2. |Archean|Archean||2813 +/- 3 Ma (Krapez et al. 2000).|||Unconformably overlies Black Flag Group.||
19889|White Flag Formation|67198|5|Briefly described|p5 fig 2, p82|Neoarchean|Neoarchean|Kalgoorlie Terrane.|2690 +/- 9 Ma|Kalgoorlie Sequence||Overlies Spargoville Formation, unconformably overlain by Black Flag Formation|Sedimentary rocks (coarse conglomerate and sandstone)|11-SEP-17
19889|White Flag Formation|68154|5|Briefly described|p160||||2690 +/- 9 Ma (igneous clast).||||A thick, felsic volcanic, volcaniclastic and siliciclastic sequence.|
19889|White Flag Formation|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Kalgoorlie Sequence.||Overlain by Black Flag Formation. Underlain by Spargoville Formation.|Felsic volcanic/volcaniclastic rocks with felsic intrusive rocks.|
19889|White Flag Formation|70773|5|Briefly described|p18 fig 11|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane.||Kalgoorlie Sequence||Overlies the Spargoville Formation. Unconformably overlain by the Black Flag Formation.|Dacite, rhyolite and volcaniclastic rocks.|
19889|White Flag Formation|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.||||||
19889|White Flag Formation|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Spargoville Formation. Overlain by the Black Flag Formation.||
19889|White Flag Formation|71308|5|Briefly described|p711 Fig.2|||Kalgoorlie Terrane.|2690 Ma.|Kalgoorlie Sequence.||||
19889|White Flag Formation|71309|6|Mentioned|p740 Fig.3|||||||||
19889|White Flag Formation|72485|6|Mentioned|p3 Fig.2|||||Kalgoorlie Sequence.||||
19889|White Flag Formation|72491|5|Briefly described|p8, 19|||Kalgoorlie Terrane, Yilgarn Craton. The basal regional unconformity is dated ~2673 Ma.||||Unconformably overlies Black Flag Formation.|Coarse clastic turbiditic sediments.|
19889|White Flag Formation|72814|4|Described|p202 Fig. 4|||East of Zuleika Shear, Ora Banda Domain and West of Zuleika Shear, Coolgardie Domain. Mineralised.||||Intruded by Star Trek Dolerite & Gabbro and Powder Sill. Mineralised quartz porphyry intrusions shown fig 4.|Intermediate volcaniclastic with andesitic crystal tuff and andesite|
19889|White Flag Formation|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
19889|White Flag Formation|73391|4|Described|vii, 19-20, 26, 50-51, 54, 58-68, 78-83|||See also p86, 91, 100-102, 105-110, 127, 131, 147, 160, 178-182, 184-185, 194, 196-197, 199, 202-203, 214, 217-218, 231, 235-236, 238-239, 241, 245-247, 284-286, 304, 310, 319, 329-330, 332-333, 338-340, 347, 349, 362, 417, 419-420, 441-443, 445, Appendices. Hunter (1993). Ora Banda Domain, Eastern Goldfields Province. The type section is at White Flag Lake. An alternative age of syn-depositional andesitic conglomerate of 2690 +/- 9 Ma is also given. Total estimated thickness is 3600m. In previous works, was overlain by Black Flag Formation and unconformably by Kurrawang Formation; here overlain gradationally by Gibson-Honman formation. Time-correlates with Ballarat Grit/Conglomerate. Lithology described in detail; partial stratigraphic column, photographs, photomicrographs, drill hole section. Sub-marine lava dome complex.|2686 +/- 5 Ma.|Black Flag Group.||Overlies Victorious Basalt,  Black Flag Series, Spargoville Formation and Talbot formation/Centenary Shale gradationally (locally unconformably).|Intermediate volcanics, basal conglomerate; intercalated fine-medium grained quartzo-feldspathic sandstone; rare andesite sills; andesitic conglomerate and breccia.|
19889|White Flag Formation|73596|6|Mentioned|p1159-1160, 1162|Neoarchean|Neoarchean|Kalgoorlie-Kambalda area.|c.2680 Ma.|Black Flag Group.||Overlies Talbot Formation. Is overlain by Gibson-Honman Formation.||
19898|White Mountain Formation|23821|4|Described|p245|Miocene|Miocene|Geological Province: Ord Basin. Maximum thickness: 113m.||||||
19898|White Mountain Formation|30862|6|Mentioned|p26|||Middle Tertiary age||||||
19898|White Mountain Formation|31529|6|Mentioned|p95|||||||||
19898|White Mountain Formation|34548|6|Mentioned|p134|||See also p137. Miocene - Pliocene||||||19-DEC-06
19898|White Mountain Formation|36213|6|Mentioned|p86|||||||||
19898|White Mountain Formation|36257|6|Mentioned|Table 2.1|||||||||
19898|White Mountain Formation|36551|6|Mentioned|Table 16|||||||||
19898|White Mountain Formation|36890|3|Fully described|p398|||Formerly White Mount Series.||||||19-DEC-06
19898|White Mountain Formation|40605|6|Mentioned|p196|||||||||
19898|White Mountain Formation|41864|2|Defined|p153|Miocene||Formerly "White Mountain Series"||||||
19898|White Mountain Formation|41866|5|Briefly described|Map legend|Cenozoic||||||||19-NOV-08
19898|White Mountain Formation|42829|5|Briefly described|p148|||||||||
19898|White Mountain Formation|43606|5|Briefly described|p5||Early Miocene|||||||
19898|White Mountain Formation|44221|14|Not recorded|p.87, 88, 97, 102|||||||||
19898|White Mountain Formation|44222|14|Not recorded|p119|||||||||
19898|White Mountain Formation|44317|4|Described|Table 4||Cenozoic|||||||19-NOV-08
19898|White Mountain Formation|44318|14|Not recorded|map legend||Tertiary|Tertiary.||||||
19898|White Mountain Formation|45022|6|Mentioned|p.165.|Pliocene|Miocene|||||||
19898|White Mountain Formation|48925|6|Mentioned|p13|||Miocene ? Fauna||||||
19898|White Mountain Formation|60703|6|Mentioned|p725 Fig. 18|Tertiary|Tertiary|||||||12-APR-05
19898|White Mountain Formation|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlies detrital ferricrete; underlies Birdum Creek beds. Thickness: 120m. Geological Province: Ord and Wiso Basins.||||||
19898|White Mountain Formation|67860|5|Briefly described|p416 Fig.4-84, p417 fig 4-85|Miocene|Miocene|See also p418 Tb. 4-18, p422. 30-115 m thick in small outcrops. Type section details given. Contains the foraminifer Ammonia beccarii.|||||Fossiliferous chert, siltstone, sandstone, marl.|
19898|White Mountain Formation|71754|14|Not recorded|p200|Pliocene|Miocene|Ref to Traves, 1955.||||||
19908|White Rocks Lamproite|41158|6|Mentioned|Table 55|||||||||
19928|Whitewater Volcanics|22474|5|Briefly described|p21||Orosirian|Age: 1855 +/- 5 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|22526|6|Mentioned|Fig3 P682||Orosirian|||||||
19928|Whitewater Volcanics|22547|4|Described|p9||Orosirian|In the Lamboo Complex, Halls Creek Orogen. Age: 1850 +/- 5 Ma. Part of the Whitewater Volcanics reassigned to Castlereagh Hill Porphyry. Overlies Marboo Formation, overlain by O'Donnell Formation||||||08-MAY-15
19928|Whitewater Volcanics|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Intruded by Paperbark supersuite.||||||14-NOV-06
19928|Whitewater Volcanics|22741|5|Briefly described|P20, Table3 P19||Proterozoic|||||||
19928|Whitewater Volcanics|22754|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Age c. 1855 Ma (Gellatly et al, 1975).||||||07-NOV-08
19928|Whitewater Volcanics|23125|5|Briefly described|Table.1|||||||||
19928|Whitewater Volcanics|23323|5|Briefly described|p454 Fig.2, p456 Tb. 1|Orosirian|Orosirian|Age: 1860-1850 Ma and 1855+/-5Ma.||||||07-FEB-07
19928|Whitewater Volcanics|23383|6|Mentioned|p8|||||||||
19928|Whitewater Volcanics|23621|5|Briefly described|p20|||||||||
19928|Whitewater Volcanics|23722|4|Described|p8|Orosirian|Orosirian|Age: 1850+/-5Ma (U-Pb zircon).   Geological Province: Hooper Complex||||||
19928|Whitewater Volcanics|23751|4|Described|p7|Paleoproterozoic|Paleoproterozoic|Age: 1855+/-5 Ma (SHRIMP U-Pb zircon). Dacitic to rhyolite ignimbrites. Geological Province: Lamboo Complex.||||||07-NOV-08
19928|Whitewater Volcanics|24173|5|Briefly described|p15, 19|||Overlain by Speewah Group; unconformably overlies Marboo Formation. Geological Province: Halls Creek Orogen. Age: 1880-1845Ma. Intruded by Mount Christine Granitoid||||||06-APR-05
19928|Whitewater Volcanics|24197|5|Briefly described|p23, p85|||Of the Paperbark Supersuite. Felsic and phenocryst-rich. Age: 1850-1860Ma. Geological province: Kimberley Province (East and West). See also p89-90 Tb. 11.1.||||||07-FEB-11
19928|Whitewater Volcanics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained quartz-feldspar rhyolite- to dacite-porphyry and welded ignimbrite; minor agglomerate, lapilli tuff and volcaniclastic rock.  Age: 1865-1850Ma.||||||07-NOV-08
19928|Whitewater Volcanics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
19928|Whitewater Volcanics|30097|6|Mentioned|Fig.54|||Also Tables 23,24,27||||||
19928|Whitewater Volcanics|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|30526|6|Mentioned|p112|||||||||
19928|Whitewater Volcanics|30533|3|Fully described|p12|||On Table 1. Dated as 1830 or 1960m.y.||||||
19928|Whitewater Volcanics|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
19928|Whitewater Volcanics|30892|5|Briefly described|p96|||||||||
19928|Whitewater Volcanics|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|30896|4|Described|p12|||Lower Proterozoic||||||
19928|Whitewater Volcanics|30897|4|Described|p9|||||||||
19928|Whitewater Volcanics|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|31393|6|Mentioned|Pl.25|||||||||
19928|Whitewater Volcanics|32108|6|Mentioned|Fig.1|||||||||
19928|Whitewater Volcanics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|32660|5|Briefly described|Table 1|||||||||
19928|Whitewater Volcanics|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
19928|Whitewater Volcanics|32699|5|Briefly described|Map legend|Carpentarian|Carpentarian|Acid lava, tuff, intrusive quartz-feldspar porphyry.||||||02-DEC-04
19928|Whitewater Volcanics|32701|5|Briefly described|Table 1|||Carpentarian. Lamboo Complex||||||
19928|Whitewater Volcanics|32728|5|Briefly described|p27|||See also Fig.3||||||
19928|Whitewater Volcanics|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|33377|6|Mentioned|Table 1|||Strat.||||||
19928|Whitewater Volcanics|33443|6|Mentioned|p260|||||||||
19928|Whitewater Volcanics|34462|6|Mentioned|p12|||?Subsurface||||||
19928|Whitewater Volcanics|34834|6|Mentioned|p213|||||||||
19928|Whitewater Volcanics|35950|6|Mentioned|p302|||||||||
19928|Whitewater Volcanics|36225|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|36308|6|Mentioned|p212|||||||||
19928|Whitewater Volcanics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|36551|6|Mentioned|p41|||||||||
19928|Whitewater Volcanics|36885|3|Fully described|p172|||||||||
19928|Whitewater Volcanics|36902|6|Mentioned|p11|||||||||
19928|Whitewater Volcanics|37299|6|Mentioned|Fig.1|||||||||
19928|Whitewater Volcanics|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
19928|Whitewater Volcanics|38071|6|Mentioned|p104|||||||||
19928|Whitewater Volcanics|38482|6|Mentioned|Table 1|||||||||
19928|Whitewater Volcanics|39827|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19928|Whitewater Volcanics|40494|4|Described|p9|||||||||
19928|Whitewater Volcanics|41158|6|Mentioned|p19|||||||||
19928|Whitewater Volcanics|41465|6|Mentioned|p6|||See also P12||||||
19928|Whitewater Volcanics|41557|6|Mentioned|p589|||||||||
19928|Whitewater Volcanics|41575|6|Mentioned|p592|||||||||
19928|Whitewater Volcanics|41961|6|Mentioned|Table 1 P39|||||||||
19928|Whitewater Volcanics|41976|4|Described|p461|||||||||
19928|Whitewater Volcanics|41977|4|Described|p471|||||||||
19928|Whitewater Volcanics|42149|6|Mentioned|p704|||||||||
19928|Whitewater Volcanics|42329|5|Briefly described|p5|||Age 1850 +/- 5 Ma. See also Fig.2 p6.||||||14-NOV-06
19928|Whitewater Volcanics|42342|5|Briefly described|p22|||||||||
19928|Whitewater Volcanics|42710|5|Briefly described|map legend|Proterozoic||||||||
19928|Whitewater Volcanics|42768|6|Mentioned|p7|||||||||
19928|Whitewater Volcanics|42811|4|Described|p7|||Of Hooper Complex.||||||14-NOV-06
19928|Whitewater Volcanics|42814|4|Described|p6|||||||||
19928|Whitewater Volcanics|42815|5|Briefly described|map|||||||||
19928|Whitewater Volcanics|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1855 Ma.||||||
19928|Whitewater Volcanics|43561|6|Mentioned|Fig.6,p1437|||Emplaced approx. Age: 1865-1850 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|43568|6|Mentioned|p506|||Dated at : 1850+/-5 Ma||||||
19928|Whitewater Volcanics|43586|6|Mentioned|Fig.1,p4|||||||||
19928|Whitewater Volcanics|43595|5|Briefly described|p350,351,443|||U-Pb zircon dates: 1850+/-5 Ma||||||
19928|Whitewater Volcanics|43632|6|Mentioned|p10|||||||||
19928|Whitewater Volcanics|43666|6|Mentioned|p6|Proterozoic|Mesoproterozoic|||||||
19928|Whitewater Volcanics|43749|6|Mentioned|p31|||||||||
19928|Whitewater Volcanics|43794|5|Briefly described|p319-320||Proterozoic|||||||
19928|Whitewater Volcanics|43819|6|Mentioned|Table 2,p33|||||||||
19928|Whitewater Volcanics|43853|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|43854|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
19928|Whitewater Volcanics|43931|5|Briefly described|p21||Orosirian|Age: 1855 +/- 5 Ma.||||||14-NOV-06
19928|Whitewater Volcanics|44140|5|Briefly described|p295 Tb.4-1, p297, p299|||||||Is overlain disconformably by O'Donnell Formation (Speewah Group), and unconformably by Revolver Creek Formation.|Acid volcanics.|
19928|Whitewater Volcanics|44155|4|Described|p234 Tb.3-2, p236 Fig.3-35,p237|Paleoproterozoic|Paleoproterozoic|See also p240-243, p247-249, p253-254. Dow and Gemuts (1969). Comagmatic with Castlereagh Hills, Bickleys and Mount Disaster Porphyries. Up to 2km thick. Contains Woodward Dolerite cobbles near base. Zircon U-Pb age from a felsic volcanic. Page (1976) recalculated data of Bofinger (1967) to obtain a whole-rock Rb-Sr isochron age of 1764 +/- 35 Ma. Other ages given.|1850 +/- 5 Ma (Page and Hancock, 1988).|Lamboo Complex, Hooper Complex||Intrudes or unconformably overlies Halls Creek Group. Intruded by Castlereagh Hill and Little Gold River Porphyries; also by Bow River and Lennard Granites. Overlain by Speewah Group.|Rhyolitic to andesitic ashflow tuff; minor intercalations of agglomerate, siltstone, sandstone, conglomerate and chert near top of sequence; rare lavas.|
19928|Whitewater Volcanics|44230|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|44231|5|Briefly described|Map Legend||Paleoproterozoic|Dacite and rhyodacite lava, tuff, agglomerate and minor volcaniclastic sedimentary rocks; commonly crystal-rich; thin pebble conglomerate at base.  Age: 1865-1850Ma. In the Hooper Complex and Lamboo Complex western zone (Bow River batholith).||||||28-SEP-11
19928|Whitewater Volcanics|44317|4|Described|Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
19928|Whitewater Volcanics|44363|5|Briefly described|p.6,7,9,11,12,13-29|||(Carpentarian).||||||
19928|Whitewater Volcanics|44364|14|Not recorded|map legend|||||||||
19928|Whitewater Volcanics|44366|14|Not recorded|p.13, Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
19928|Whitewater Volcanics|44397|14|Not recorded|p.9,18,19, Table 2||Carpentarian|||||||
19928|Whitewater Volcanics|44398|14|Not recorded|map legend||Carpentarian|||||||
19928|Whitewater Volcanics|44868|5|Briefly described|Map Legend||Proterozoic|||||||
19928|Whitewater Volcanics|45038|14|Not recorded|p.27||Precambrian|||||||
19928|Whitewater Volcanics|45047|2|Defined|p69|Carpentarian|Carpentarian|See also p27.||||||14-NOV-06
19928|Whitewater Volcanics|45048|6|Mentioned|p63|||||||||
19928|Whitewater Volcanics|45050|6|Mentioned|p7|||||||||
19928|Whitewater Volcanics|45112|5|Briefly described|p48|||||||||
19928|Whitewater Volcanics|45140|6|Mentioned|p12-13, p21|||Kimberley region.|~1900 Ma.|||||
19928|Whitewater Volcanics|46797|4|Described|p80|||Dates given||||||
19928|Whitewater Volcanics|46864|6|Mentioned|p39|||Age dates discussed.||||||
19928|Whitewater Volcanics|48931|3|Fully described|p20|||||||||
19928|Whitewater Volcanics|48938|4|Described|p9|||See also p13.||||||14-NOV-06
19928|Whitewater Volcanics|48950|6|Mentioned|p36|||||||||
19928|Whitewater Volcanics|50437|5|Briefly described|p1.5, 2.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1854-1855 +/- 5Ma (Shrimp), 1850 +/- 3Ma (U-Pb con.).||||||07-NOV-08
19928|Whitewater Volcanics|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Of Lamboo Complex. Unconformably overlies Halls Creek Group. Porphyritic rhyolite, rhyodactite||||||07-NOV-08
19928|Whitewater Volcanics|60283|5|Briefly described|p25 Fig.2|||Halls Creek Orogen.|c.1855 Ma.||||Felsic volcanism.|
19928|Whitewater Volcanics|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Co-magmatic with Paperbark Supersuite.||||||07-NOV-08
19928|Whitewater Volcanics|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Part of Lamboo Complex. Age: 1865-1850Ma. Porphyritic rhyolite and rhyodacite. Geological Province: Halls Creek Orogen.||||||07-NOV-08
19928|Whitewater Volcanics|60714|6|Mentioned|p121.|Orosirian|Orosirian|Halls Creek Orogen. Directly overlies ?glacial "boulder phyllite', implying yet another glacial episode in the Paleoproterozoic.|1855 +/- 5 Ma(U-Pb zircon: Page and Sun, 1994).|||||
19928|Whitewater Volcanics|60724|4|Described|p16, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Thick-bedded, massive, med.to fine gr. qtz-feldspar porphyry, often with pumice fragments; minor laminated vol'clastics and amyg.basalt. Unconf. on Marboo Fm; unconf.under O'Donnell Fm. Intruded by Bow batholith granite. Age:1850+/-5Ma (U-Pb). Hooper Cmplx||||||18-JUN-13
19928|Whitewater Volcanics|62715|5|Briefly described|p1753, p1779|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850Ma.||||||07-NOV-08
19928|Whitewater Volcanics|63866|5|Briefly described|p105, p129, p132-p133, p138|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Numeric age is interpreted as the crystallisation age. Comagmatic with the Castlereagh Hill Porphyry and Greenvale Porphyry.|1849 +/- 6 Ma (Worden et al, in review)|||Unconformably overlies the Marboo Formation. Overlain by the Speewah Group.|Felsic volcanics including quartz-phyric rhyolite, rhyodacite, welded ignimbrite and tuff.|
19928|Whitewater Volcanics|64104|6|Mentioned|p76 fig 10, p76|Paleoproterozoic|Paleoproterozoic|Possible source of some clasts in Duerdin Group.||||||
19928|Whitewater Volcanics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Fine- to medium-grained quartz-feldspar rhyolite- to dacite-porphyry and welded ignimbrite; minor agglomerate, lapilli tuff, and volcaniclastic rock.||||||09-DEC-08
19928|Whitewater Volcanics|64725|5|Briefly described|p75.|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen. Host to low-sulfidation adularia-sericite epithermal Au deposit.|1855 Ma.|||||
19928|Whitewater Volcanics|64730|6|Mentioned|p141|Paleoproterozoic|Paleoproterozoic|Felsic. Age from Page and Hancock 1988; Tyler et al. 1999; Griffin et al. 2000.|ca. 1855-1850 Ma.|||Unconformably overlies Marboo Formation.||03-MAY-12
19928|Whitewater Volcanics|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex and Western Zone of Hall Creek Orogen.|1860 - 1850 Ma.|||Co-magmatic with Castlereagh Hill Porphyry.||12-APR-12
19928|Whitewater Volcanics|64956|5|Briefly described|p2 Tb. 26, p95-96|Paleoproterozoic|Paleoproterozoic|Cryst. Age: 1849+/-6Ma. Geological province: Halls Creek Orogen. Sample is a K-feldspar-quartz-phyric rhyodacite - generally massive and unfoliated. The sample is dark coloured with glassy matrix; subhedral K-feldspar and quartz phenocrysts are common.||||||07-FEB-11
19928|Whitewater Volcanics|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Lamboo Complex, Halls Creek Orogen. Porphyritic rhyolite, rhyodacite||||||
19928|Whitewater Volcanics|66127|5|Briefly described|Plate 1, 2, 3, 4.|Paleoproterozoic|Paleoproterozoic||c.1855 Ma.||||Volcanic and sedimentary rocks.|
19928|Whitewater Volcanics|66845|5|Briefly described|p536, p538, p540|Paleoproterozoic|Paleoproterozoic|Unconformably overlies turbiditic quartz wacke. Western zone of Lamboo Complex. Closely related to Paperbark supersuite. Indistinguishable crystallisation ages for Paperbark supersuite, Whitewater Volcanics and related intrusions concludes the Western Zone of the Lamboo Complex is a continuation of the Hooper Complex in the west Kimberley.|c. 1855 Ma|||||
19928|Whitewater Volcanics|66846|6|Mentioned|p548, p549 Fig.2|Orosirian|Orosirian|In the Western Zone of the Lamboo Complex.||||Intruded by Paperbark supersuite granites.|Felsic volcanics.|
19928|Whitewater Volcanics|67323|5|Briefly described|p29|||Coeval with Paperbark Suite.|~1865-1850 Ma.||||Felsic volcanics.|
19928|Whitewater Volcanics|67563|6|Mentioned|p120 Fig.1|||||||||
19928|Whitewater Volcanics|68078|5|Briefly described|p5, p19|Paleoproterozoic|Paleoproterozoic|Age is age of crystallization and intrusion into marboo formation.|1855 Ma|||Unconformably overlies Marboo Formation, unconformably overlain by Speewah Group|Felsic volcanic rocks.|
19928|Whitewater Volcanics|68244|6|Mentioned|p661|||Mount House area, Kimberley region.||||||
19928|Whitewater Volcanics|68542|6|Mentioned|p12|||||||||
19928|Whitewater Volcanics|68576|5|Briefly described|Q_2: p12|||Kimberley region. Same age as Leichhardt Volcanics in the Mount Isa region; possibly part of a vast array of coalescing caldera fields across northern Australia.|||||Felsic tuffs.|
19928|Whitewater Volcanics|69003|5|Briefly described|p5, p18-19|Paleoproterozoic|Paleoproterozoic|W zone, Lamboo Province, Halls Creek Orogen.|c.1855 Ma.|||Overlies Marboo Formation.||
19928|Whitewater Volcanics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Age from OZCHRON1. Comment: 'This is an excellent age for igneous crystallisation of the Whitewater Volcanics. It agrees with the conventional age (1850+/-5) and with the Whitewater age in the West Kimberley (1854+/-5) where Whitewater Volcanics are intruded by 1864-1852 Ma granite.'|crystallisation age 1857+/-4 Ma U/Pb SHRIMP|Paperbark Supersuite|Includes 3 unnamed units.||porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated|
19928|Whitewater Volcanics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1850-1857 Ma|Paperbark Supersuite|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock. Coarse grained feldspathic sandstone and pebble conglomerate.|
19928|Whitewater Volcanics|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Halls Creek Orogen.||||Is intruded by Bow River Granite.||12-JUL-16
19928|Whitewater Volcanics|69422|5|Briefly described|p7:1-3|Orosirian|Orosirian|Western Zone, Halls Creek Orogen. Considered to be comagmatic with Bow River Granite (Paperbark Supersuite). Deformed, metamorphosed and intruded during the 1865-1850 Hooper Orogeny. SHRIMP U-Pb zircon age; agrees with WA ages.|1849 +/- 6 Ma (Worden et al., 2008).|||Unconfortmably overlies Marboo Volcanics. Is intruded by Bow River Granite.|Red-brown porphyritic rhyolite and rhyodacite; angular phenocrysts of quartz and feldspar up to 2-4mm long. Ignimbrites predominate over lava flows: probably subaerial.|12-JUL-16
19928|Whitewater Volcanics|69435|6|Mentioned|p20:4|||||||Is overlain unconformably by Legune Formation.||12-JUL-16
19928|Whitewater Volcanics|69452|6|Mentioned|p36:6|||Halls Creek Orogen.||||Is overlain unconformably by Ragged Range Conglomerate and Kellys Knob Sandstone.||12-JUL-16
19928|Whitewater Volcanics|69585|5|Briefly described|p4, p7|Orosirian|Orosirian|Western Lamboo Province.|c.1855 Ma.|||Is overlain unconformably by O'Donnell Formation (Speewah Group).||
19928|Whitewater Volcanics|69597|5|Briefly described|p3, p5 fig 2b|Paleoproterozoic|Paleoproterozoic|Western Lamboo Province. Thought to have formed by partial melting of Paleoproterozoic to Archean imtermediate to felsic rocks.|1855-1850 Ma|Paperbark Supersuite||||
19928|Whitewater 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; 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, 250k_interpgeop_lut.csv.|1864-1854 Ma (Inferred)|Unit of Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated, coarse-grained feldspathic sandstone and pebble conglomerate|
19928|Whitewater Volcanics|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|1862 - 1854 Ma; Griffin et al. (2000).|Unit in Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.|1864-1854 Ma (Griffin et al., 2000).|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1854-1864 Ma|Paperbark Supersuite|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.Metadacite and meta rhyodacite..|
19928|Whitewater Volcanics|70206|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Lamboo Complex|||Porphyritic rhyolite, rhyodacite.|
19928|Whitewater Volcanics|70731|5|Briefly described|p267-268,274,276,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Felsic volcanics and volcaniclastics intepreted to be the last period of felsic magmatism. In contact with Speewah Group. Felsic equivalent to Paperbark Supersuite.|c. 1855 Ma|||Underlain by Marboo Formation.||
19928|Whitewater Volcanics|70812|5|Briefly described|p3, p6-p7, p19-p20, p29, p38|Orosirian|Orosirian|Age derived from cogenetic relationship with the Paperbark Supersuite. This unit may have formed as a result of extensional processes towards the end of the Hooper Orogoney. Hosts occurrences of Au, Ag, Pb, Cu, Mo and Zn.||||Overlies the Marboo Formation.|Felsic volcanic and volcaniclastic rocks.|
19928|Whitewater Volcanics|70851|5|Briefly described|p3-p5, p16, p20, p24, p29, p35|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Geophysical response is discussed.|c. 1855 Ma|Paperbark Supersuite||||28-MAR-23
19928|Whitewater Volcanics|71113|5|Briefly described|p96,99|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Developed during extension and partial melting toward the end of the Hooper Orogeny.|c. 1855 Ma|||Underlain unconformably by Marboo Formation.||
19928|Whitewater Volcanics|71140|6|Mentioned|p96, 99|Orosirian|Orosirian|Western Zone, Lamboo Province, Halls Creek Orogen. Produced by extension and partial melting toward the end of the Hooper Orogeny.|c.1855 Ma.|||Unconformably overlies Marboo Formation.|Felsic volcanic rocks.|
19928|Whitewater 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); 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, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1864 to 1854+\-5 Ma (inferred-isotopic)|Unit of Paperbark Supersuite.|||Thick-bedded, massive fine- to medium-grained quartz-feldspar rhyolite to dacite porphyry and welded ignimbrite; minor agglomerate, lapilli tuff, dacitic and rhyodacitic ash-flow tuff, and volcaniclastic sedimentary rock, minor siltstone interbeds.|
19928|Whitewater Volcanics|71281|4|Described|p421-422|Paleoproterozoic|Paleoproterozoic|Lamboo Province. Generated at the peak of the 1870-1850 Ma Hooper Orogeny. Age also given as c.1855 Ma.|1864-1852 Ma.|Paperbark Supersuite.||Is overlain unconformably by O'Donnell Formation (Speewah Group).|Late-stage erupted felsic-rich volcanics.|
19928|Whitewater Volcanics|71397|4|Described|p2,5|Orosirian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Considered to be the volcanic and subvolcanic equivalent to plutonic rocks in the Paperbark Supersuite 9see p2 for references). Three samples from Whitewater Volcanics yielded igneous crystallisation dates of 1854+\-5, 1854+\-6 and 1857+\-4 Ma, suggest contemporaneous felsic volcanism over a strike length >600 km (Griffin et al., 2000a).|c. 1854 Ma|Unit of Paperbark Supersuite.|||Volcaniclastic rocks interlayered with felsic to intermediate volcanic rocks.|
19928|Whitewater Volcanics|71592|5|Briefly described|Appendix A.|||Halls Creek Orogen.|1849+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
19928|Whitewater Volcanics|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.|1857 - 1849 Ma.|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal-rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|71873|5|Briefly described|p426,442-443|Orosirian|Orosirian|Geological province: Lamboo Province. Deformed by Hooper Orogeny c. 1860 Ma. 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.|c. 1860-1850 Ma|Unit of Paperbark Supersuite.||Intruded into Marboo Formation.||
19928|Whitewater Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|Max age ~1864, Min age 1854+/-5 Ma.|Paperbark Supersuite.|||Porphyritic rhyolite to dacite; coherent lavas, subvolcanic intrusions, and pyroclastic deposits; commonly crystal rich; minor volcanic breccia, lapilli tuff, and volcaniclastic rock; locally foliated.|
19928|Whitewater Volcanics|72437|5|Briefly described|p5, p9, p24, p27, p33|Palaeoproterozoic|Palaeoproterozoic|Hooper Complex and Lamboo Complex. Previously described in Gellatly et al (1975), Griffin and Sheppard et al (1997). Comagmatic with rocks of the Paperbark Supersuite and the Greenvale Porphyry and Castlereagh Hill Porphyry. Alteration and low-grade metamorpism is widespread but textures are almost without exception igneous.|c. 1855|||||
19928|Whitewater Volcanics|72490|6|Mentioned|p3|Orosirian|Orosirian|Lamboo Province.|ca. 1855 Ma|||Underlain by Marboo Formation.|Felsic volcanic rocks.|
20020|Wilga Coal Measures|46849|6|Mentioned|p178|||||||||
20060|Wilkinson Range beds|39340|6|Mentioned|p359|||||||||
20060|Wilkinson Range beds|43205|5|Briefly described|map legend||Paleozoic|Permian age?||||||07-NOV-08
20060|Wilkinson Range beds|70772|6|Mentioned|p11|Permian|Permian|Officer Basin. Age is a detrital zircon maximum depositional age.|||||Tillites.|
20060|Wilkinson Range beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, claystone, tillite|
20060|Wilkinson Range beds|71618|6|Mentioned|p129|Permian|Permian|Correlatable to Lower Permian diamictites in the Madura Shelf.||||||05-SEP-19
20068|Willangie beds|45153|6|Mentioned|App.4-58|||||||||
20070|Willara Formation|7433|6|Mentioned|p25 Fig.2, p28 Fig.5. |Ordovician|Ordovician|Canning Basin. Marine carbonates.||||||
20070|Willara Formation|13255|6|Mentioned|p368|Early Ordovician|Early Ordovician|Roebuck Basin.||||Overlies Nambeet Formation. Is overlain by Goldwyer Formation.||
20070|Willara Formation|13995|5|Briefly described|p67, p87, p101|Ordovician|Ordovician|Canning Basin. Graptolite species.||||Is overlain conformably or disconformably by Goldwyer Formation.|Includes bedded limestones.|
20070|Willara Formation|14228|5|Briefly described|p6 fig3|Middle Ordovician|Early Ordovician|Canning Basin.||||Overlies Nambeet Formation. Overlain by Goldwyer Formation.||06-OCT-16
20070|Willara Formation|22646|6|Mentioned|Fig 5 on p 105|Early Ordovician|Early Ordovician|Canning Basin.  Age - Arenig.||||||
20070|Willara Formation|22650|5|Briefly described|p 160|Ordovician|Ordovician|Province - Canning Basin.||||||
20070|Willara Formation|22718|5|Briefly described|P4, Table1 P7||Early Ordovician|||||||
20070|Willara Formation|22738|4|Described|5,11,12,16, map|Early Ordovician|Early Ordovician|Max thickness 750 m. Overlain by Goldwyer Formation, Grant Group; underlain by Nambeet Formation.||||||13-NOV-07
20070|Willara Formation|22741|6|Mentioned|P21|||||||||
20070|Willara Formation|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
20070|Willara Formation|22765|5|Briefly described|P7, Table1||Arenig|Overlain by Goldwyer Formation.||||||13-NOV-07
20070|Willara Formation|22767|5|Briefly described|Table3 P18, P11||Ordovician|||||||
20070|Willara Formation|22801|5|Briefly described|P10, Table1 P9||Early Ordovician|||||||
20070|Willara Formation|22814|5|Briefly described|fig2|Ordovician|Ordovician|||||||
20070|Willara Formation|23212|4|Described|Table.1 p6||Early Ordovician|||||||
20070|Willara Formation|24061|4|Described|p176|Early Ordovician|Early Ordovician|Formerly Thangoo Formation. Geological Province:  Canning Basin.||||||
20070|Willara Formation|24390|6|Mentioned|p8|||Geological Province: Canning Basin.||||||
20070|Willara Formation|24449|5|Briefly described|p741 Fig. 2|Llanvirnian|Arenigian|Age: ~475m.y.  Geological Province: Canning Basin.||||||
20070|Willara Formation|33738|6|Mentioned|p55|||||||||
20070|Willara Formation|33965|4|Described|Table 1|||||||||
20070|Willara Formation|35119|4|Described|p465|||Mention Text-Fig.3.||||||
20070|Willara Formation|36257|6|Mentioned|Table 2.1|||||||||
20070|Willara Formation|36438|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|36634|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|Early to Middle OrdovicianE - M||||||
20070|Willara Formation|36890|3|Fully described|p323|||Formerly Thangoo Limestone.||||||13-NOV-07
20070|Willara Formation|37368|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|37369|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|37370|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|38732|6|Mentioned|p33|||||||||
20070|Willara Formation|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|38886|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|39854|6|Mentioned|p21|||||||||
20070|Willara Formation|39857|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
20070|Willara Formation|40078|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|Early to Middle OrdovicianE - M||||||
20070|Willara Formation|40136|5|Briefly described|p43|||||||||
20070|Willara Formation|40992|6|Mentioned|Fig.11|||||||||
20070|Willara Formation|41169|6|Mentioned|p140|||||||||
20070|Willara Formation|41209|6|Mentioned|p143|||||||||
20070|Willara Formation|41215|6|Mentioned|p265|||||||||
20070|Willara Formation|41730|6|Mentioned|p472|||||||||
20070|Willara Formation|41854|5|Briefly described|p94|||||||||
20070|Willara Formation|41913|6|Mentioned|Fig.2 P107|||||||||
20070|Willara Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
20070|Willara Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
20070|Willara Formation|42930|5|Briefly described|Fig.1 p473|Ordovician|Ordovician|Conformably overlies Nambeet Formation;conformable below and interfingers with Goldwyer Formation. Geological Province: Canning Basin.||||||13-NOV-07
20070|Willara Formation|43563|6|Mentioned|p4|Llanvirnian|Arenigian|||||||
20070|Willara Formation|43656|6|Mentioned|Fig.2,p8|Llanvirnian|Arenigian|||||||
20070|Willara Formation|43666|6|Mentioned|p19||Arenigian|||||||
20070|Willara Formation|43746|6|Mentioned|Fig.2,p11|Llanvirnian|Arenigian|||||||
20070|Willara Formation|43803|6|Mentioned|p65||Ordovician|||||||
20070|Willara Formation|43815|6|Mentioned|Table 2,p95-96|||||||||
20070|Willara Formation|43818|6|Mentioned|Fig.2.p39||Early Ordovician|||||||
20070|Willara Formation|44143|4|Described|p426, p428, 441 Table 4-19|Early Ordovician|Early Ordovician|Up to 532m thick; limestone & dolomite; shallow marine. Conformably overlies Wilson Cliffs Sandstone, Nambeet and Carranya Formations; is conformably overlain by Goldwyer Formation. Type section between 2,610 and 3,142 m in Willara 1 (MUNRO: 19deg 10' 48" S, 122deg 04' 14" E). Contains conodonts, graptolites & microflora; Arenigian to early Llanvirnian.||||||24-NOV-17
20070|Willara Formation|44356|6|Mentioned|p8||Early Ordovician|||||||
20070|Willara Formation|44357|5|Briefly described|p11,Tb.1 p10||Early Ordovician|Assumed present from seismic evidence and drilling in adjacent sheets.||||||
20070|Willara Formation|45153|2|Defined|App.1-4|Early Ordovician|Early Ordovician|Formerly Thangoo Limestone.||||||
20070|Willara Formation|45158|3|Fully described|p28|||||||||
20070|Willara Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
20070|Willara Formation|50085|5|Briefly described|p8|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
20070|Willara Formation|50089|5|Briefly described|p427, p430 Fig. 5|Ordovician|Ordovician|Contains Oepikodus cleftus (conodont) in lower level. Geological Province: Amadeus Basin. See also p431.||||||
20070|Willara Formation|61020|6|Mentioned|p33 Fig. 4|||Lead for petroleum potential.  Geological Province: Canning Basin.||||||20-APR-05
20070|Willara Formation|61021|5|Briefly described|p36 Fig. 2|Arenigian|Arenigian|Geological Province: Canning Basin.||||||17-DEC-07
20070|Willara Formation|61551|6|Mentioned|p351 Fig.2. |Darriwilian|Tremadocian|||||Overlies Nambeet Formation.||
20070|Willara Formation|62794|6|Mentioned|p298.|Early Ordovician|Early Ordovician|Canning Basin. Middle correlated with Horn Valley Siltstone, Amadeus Basin (Webby et al 1981).||||||
20070|Willara Formation|62982|5|Briefly described|p7|Ordovician|Ordovician|Contains the Acacia Sandstone Member. Bioturbated carbonate and mudstone deposits; richly fossiliferous. Overlies Nambeet Formation; overlain by Goldwyer Formation. Geological Province: Canning Basin.||||||16-JAN-07
20070|Willara Formation|64185|5|Briefly described|p158 Fig. 2, p159, p163, p165, p166-167|Early Ordovician|Early Ordovician|Underlain by Nambeet Formation conformably, overlain by Goldwyer Formation, conformably. Max thickness: 450m. Marine. See p163 for more information.||||||
20070|Willara Formation|64186|4|Described|p169, p171, p170 Fig. 1|Early Ordovician|Late Cambrian|Overlain by Goldwyer Formation, underlain by Nambeet Formation. Max thickness: 532m. An open platform facies carbonate sequence with minor sandstone interbeds. Conformably overlies basal sandstone.||||||
20070|Willara Formation|64334|5|Briefly described|p39-41, 43|Ordovician|Ordovician|Canning Basin; subsurface only. Arenig.|||Acacia Sandstone Member.|Overlies Nambeet Formation. Is overlain by Goldwyer Formation. Correlates with Prices Creek Group.|Limestone; minor sandstone. Fossiliferous.|
20070|Willara Formation|64513|5|Briefly described|p23,p24, p26 Fig 3, p28, p33-35.|Middle Ordovician|Early Ordovician|Canning Basin. Unit description taken from lithologs diagram on p26 Fig3. Acritarchs described from 4 wells. Also contains conodonts, graptolites and trilobites. Fauna indicates age range described as early Arenig to early Llanvirn. [equivalent to Floian to Darriwilian].||||Overlies Nambeet Formation and conformably underlies Goldwyer Formation.|Includes alternating layers of limestone, lesser shale; minor claystone in the upper parts.|
20070|Willara Formation|64643|5|Briefly described|p3 Fig. 2|Middle Ordovician|Middle Ordovician|||||||
20070|Willara Formation|64982|5|Briefly described|p699 Fig.4, p701.|Arenig|Arenig|Carbonate-dominated transgressive sequence, c. 300 m thick, deposited on inner carbonate ramps and shallow tidal flats. Fossiliferous. Acts as seal for Acacia Sandstone hydrocarbon reservoir.|||Includes Acacia Sandstone.|Overlies Nambeet Formation. Is overlain by Goldwyer Formation.|Limestones, shales and interbedded limestone and shale, with the Acacia Sandstone in the upper part of the unit.|
20070|Willara Formation|65301|5|Briefly described|p3, p5 Fig. 4|Middle Ordovician|Middle Ordovician|Contains the Acacia Sandstone Member locally. Geological province: Canning Basin, Broome Platform. Predominantly carbonate unit. See also p8 Fig. 5.||||||
20070|Willara Formation|65449|5|Briefly described|p3-6, p10, p37|Middle Ordovician|Early Ordovician|Fossiliferous marine unit. Oil was recovered from this unit in Leo 1; geochemical analysis indicated Bongabinni Formation source.|||Acacia Sandstone Member.|Overlies Nambeet Formation. Is overlain by Goldwyer Formation.||
20070|Willara Formation|68007|5|Briefly described|p2, p4-5, p13, Plate 1|Middle Ordovician|Middle Ordovician|Canning Basin. Fossiliferous marine unit; contains the alga G. prisca.||||Overlies Nambeet Formation. Is overlain by Goldwyer Formation.||26-FEB-20
20070|Willara Formation|68902|6|Mentioned|p9 fig 5, p22-23|Ordovician|Ordovician|Forms a useful seismic reflector.||||Overlies Nambeet Formation, overlain by Goldwyer Formation.||
20070|Willara Formation|69029|6|Mentioned|p319-320|Darriwilian|Tremadocian|Of Canning Basin.||||Overlain by Goldwyer Formation.Overlain by the Carribuddy Group. Underlain by Nambeet Formation.||04-SEP-19
20070|Willara Formation|69182|5|Briefly described|Ch4 p9-p12, Ch4 p20-p25, Ch4 p30-p35|Middle Ordovician|Early Ordovician|Canning Basin. Poor prospectivity as a carbon dioxide reservoir due to poor permeability. Incorrectly referred to as the Willara Group in Ch4 p93. See also Ch4 p38-p41, Ch4 p44-p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p64-p65, Ch4 p67, Ch4 p74, Ch4 p79-p82, Ch4 p92-p96.|||Includes the Acacia Sandstone Member.|Overlies the Nambeet Formation. Overlain by the Goldwyer Formation.|Dolomitic carbonates and some sandstone.|11-FEB-20
20070|Willara Formation|69297|6|Mentioned|p350|Early Ordovician|Early Ordovician|Canning Basin. Deposited under marine or supratidal conditions.||||||
20070|Willara Formation|69312|5|Briefly described|p3, p15, p19, p23 fig 26|Early Ordovician|Early Ordovician|Canning Basin. Petroleum reservoir rock that is sealed by the salts of the Carribuddy Group. See also p25 fig 30, p26 fig 32, p28 fig 36.||||Overlies the Nambeet Formation. Overlain by the Nita and Goldwyer Formations.|Carbonates.|11-FEB-20
20070|Willara Formation|69883|5|Briefly described|p1, p4-p6, p9, p14, p21-p22|Llanvirn|Arenig|Canning Basin. Deposited in a mainly open marine to intertidal environment. Assigned to supersequence A2. Age equivalent to the Wilson Cliffs Sandstone. See also p30, p41, p45, plate 1-4.|||Includes the Acacia sandstone member.|Conformably overlies the Nambeet Formation. Conformably overlain by the Goldwyer Formation. Coeval with the Wilson Cliffs Sandstone.|Dominated by limestone, with subordinate dolostone, mudstone and sandstone of shallow marine origin.|
20070|Willara Formation|70774|5|Briefly described|p4|Middle Ordovician|Middle Ordovician|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Nambeet Formation. (Unconformably?) overlies the Wilson Cliffs Sandstone.||
20070|Willara Formation|71146|5|Briefly described|p6, p12 fig 8|Middle Ordovician|Middle Ordovician|Canning Basin.|ca 485 Ma|||Overlies the Wilson Cliffs Sandstone and the Nambeet Formation. Overlain by the Goldwyer Formation.|Carbonate.|
20070|Willara Formation|71171|6|Mentioned|p1-p2, p4|||Canning Basin.|||Includes the Acacia Sandstone Member.|||
20070|Willara Formation|71870|5|Briefly described|p3, p5-p6, p10-p11, p13-p16|Darriwilian|Floian|Canning Basin.||||Overlies the Nambeet Formation. Overlain by the Goldwyer Formation.||
20070|Willara Formation|71894|5|Briefly described|p4, p6, p31|Middle Ordovician|Early Ordovician|Canning Basin.||||Overlies the Nambeet Formation. Overlain by the Goldwyer Formation.|Carbonate.|11-FEB-20
20070|Willara Formation|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|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||||Conformably overlies Nambeet Formation and unconformably overlies  Carranya Formation. Overlain by Goldwyer and Nita Formations.||
20070|Willara Formation|72499|5|Briefly described|p7 Fig.6.|Middle Ordovician|Early Ordovician|Located in the Willara Sub-basin and the Broome Platform.||||Overlies Nambeet Formation underlies Goldwyer Formation.|Includes carbonates.|
20070|Willara Formation|72500|5|Briefly described|p380-382, p389, p393-394, p396-397, p399|Darriwilian|Floian|Canning Basin.||||Conformably overlies the Nambeet Formation. Overlain by the Goldwyer Formation.|Limestone, dolostone, sandstone and shaly siltstone.|28-AUG-20
20070|Willara Formation|72503|5|Briefly described|p25, p27-30, p32|Dapingian|Dapingian|[Article discusses 7 conodonts from drill core section(s); none are age-diagnostic].||||Underlain by Nambeet Formation. Conformably overlain by Goldwyer Formation.|Richly fossiliferous carbonate and sandstone with minor mudstone.|
20070|Willara Formation|73117|5|Briefly described|p3|Middle Ordovician|Lower Ordovician|Canning Basin.||||Underlain by Nambeet Formation. Overlain by Goldwyer Formation.|Dominantly carbonate.|
20070|Willara Formation|73344|4|Described|p. 1-6, 8-9, 11, 13, 31-32, 35-38...|Dapingian|latest Floian|Canning Basin, subsurface. Defined by Playford et al. (1975) after proposal by RA McTavish. Type section is from Willara 1 well between 2610 and 3142 m [532 m thickness]. Contains a CA-ID-TIMS bentonite age of 470.18 +/- 0.13 Ma near the base. Basal 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). Part of super sequence A1. Covers part of the J. gananda conodont biozone. Biostratigraphy suggests the unit may be unconformably underlain by Wilson Cliffs Sandstone in some wells; although was said to be unlikely. More locations: p. 40-42, 44, 47, 55-56, 59, Pl.1-4.|470.18 +/- 0.13 Ma||Acacia Sandstone Member|Conformably underlain by Nambeet Formation. Overlain by Goldwyer Formation. Equivalent to Gap Creek Formation (Prices Creek Group).|Carbonate dominated.|
20070|Willara Formation|73345|6|Mentioned|p227, p230|Middle Ordovician|Middle Ordovician|Canning Basin, widespread. Potentially correlative to Barnicarndy Formation. Includes the J. gananda biozone.||||||
20070|Willara Formation|73346|6|Mentioned|p3, p27, App.1 p34|Middle Ordovician|Early Ordovician|Canning Basin. Deposited in shallow marine environments. May be age equivalent to Cobb Formation.|||Acacia Sandstone Member||Includes shallow marine sandstone.|
20070|Willara Formation|73567|5|Briefly described|p61-64, p66, p68-71|Dapingian|Floian|Canning Basin. Defined in the subsurface only. One new high precision U-Pb (CA-ID-TIMS) age of 470.18 +/-0.13 Ma was reported for a bentonite near the base of the unit.|470.18 +/-0.13 Ma U-Pb CA-ID-TIMS|||Conformably underlain by Nambeet Formation. Equivalent to the Gap Creek Formation (Prices Creek Group).|Includes limestone.|
20073|Willaraddie Formation|6944|6|Mentioned|p571 Fig.2.|Late Devonian|Late Devonian|Southern Carnarvon Basin. Famennian. Alluvial fan deposits. Laterally equivalent to braided stream deposits of Munabia Formation.||||||23-SEP-15
20073|Willaraddie Formation|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18|Famennian|Famennian|Merlinleigh Sub-basin.||||Overlies Munabia Formation. Is overlain by Moogooree Limestone.|Conglomerate, sandstone, siltstone alluvial fan.|
20073|Willaraddie Formation|23311|5|Briefly described|map legend|Famennian|Famennian|||||||
20073|Willaraddie Formation|23312|5|Briefly described|map legend|Famennian|Famennian|||||||
20073|Willaraddie Formation|23403|4|Described|p7|Early Carboniferous|Middle Devonian|A conglomeritic to sandy sequence.  Geological Province: Gascoyne Complex.||||||24-NOV-09
20073|Willaraddie Formation|23726|5|Briefly described|p34|Devonian|Devonian|Overlying unit Moogooree Limestone. Underlying unit Munabia Sandstone. Geological Province: Carnarvon Basin.||||||
20073|Willaraddie Formation|23815|4|Described|p276|Late Devonian|Late Devonian|Geological Province: Carnarvon Basin. Overlying unit: Moogooree Limestone (disconformable). Underlying unit: Munabia Sandstone (conformable). Max. thickness: 294 m.||||||
20073|Willaraddie Formation|24059|6|Mentioned|p149|||Geological Province: Carnarvon Basin.||||||15-JAN-07
20073|Willaraddie Formation|24390|5|Briefly described|p19 Fig. 10|Carboniferous|Devonian|Geological Province: Southern Carnarvon Basin.||||||
20073|Willaraddie Formation|30875|6|Mentioned|p10|||See also P14. Devonian age.||||||
20073|Willaraddie Formation|31561|5|Briefly described|p33|||Late Devonian||||||
20073|Willaraddie Formation|32648|6|Mentioned|p32|||Famennian||||||
20073|Willaraddie Formation|32865|5|Briefly described|p477|||||||||
20073|Willaraddie Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
20073|Willaraddie Formation|33386|6|Mentioned|Fig.7|||||||||
20073|Willaraddie Formation|33453|5|Briefly described|p69|||Devonian.||||||
20073|Willaraddie Formation|34085|6|Mentioned|Cor.chart|||Famennian||||||
20073|Willaraddie Formation|34203|6|Mentioned|p14|||||||||
20073|Willaraddie Formation|35282|6|Mentioned|Fig.2|||||||||
20073|Willaraddie Formation|35981|6|Mentioned|p134|||||||||
20073|Willaraddie Formation|36257|6|Mentioned|Table 2.1|||||||||
20073|Willaraddie Formation|36743|6|Mentioned|p40|||||||||
20073|Willaraddie Formation|36890|3|Fully described|p276|||||||||
20073|Willaraddie Formation|38770|4|Described|p63|||||||||
20073|Willaraddie Formation|40617|6|Mentioned|Fig.1|||||||||
20073|Willaraddie Formation|41271|3|Fully described|p52|||||||||
20073|Willaraddie Formation|41438|6|Mentioned|p102|||||||||
20073|Willaraddie Formation|41443|6|Mentioned|p159|||||||||
20073|Willaraddie Formation|41492|5|Briefly described|Fig.2|||||||||
20073|Willaraddie Formation|41512|6|Mentioned|Fig.1|||||||||
20073|Willaraddie Formation|41839|6|Mentioned|p19|||||||||
20073|Willaraddie Formation|42030|3|Fully described|p745|||||||||
20073|Willaraddie Formation|42116|5|Briefly described|p25|||||||||
20073|Willaraddie Formation|42547|5|Briefly described|p89|||||||||
20073|Willaraddie Formation|43566|6|Mentioned|Fig.3,p416|||||||||
20073|Willaraddie Formation|44344|14|Not recorded|p.5, opp. 4, map||Devonian|(G50-1).||||||
20073|Willaraddie Formation|44345|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
20073|Willaraddie Formation|44537|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
20073|Willaraddie Formation|44657|14|Not recorded|p.5,7,8|||(Willaradie).||||||
20073|Willaraddie Formation|44994|5|Briefly described|p9|||Fig.6 Correlation||||||
20073|Willaraddie Formation|45015|2|Defined|p55-60, map legend|||Quartzwacke, siltstone, quartz sandstone and conglomerate. Conformably overlies Munabia Sandstone; disconformably overlain by Moogooree Limestone. Max. thickness: >3000ft.  See also p53 Fig. 21.||||||31-MAY-06
20073|Willaraddie Formation|45016|14|Not recorded|p.9 (map)|||||||||
20073|Willaraddie Formation|45041|6|Mentioned|Fig.45|||Famennian||||||
20073|Willaraddie Formation|45063|6|Mentioned|p30|||See also Fig. 9. Dev.||||||
20073|Willaraddie Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
20073|Willaraddie Formation|46978|6|Mentioned|Fig.2|||||||||
20073|Willaraddie Formation|50085|5|Briefly described|p19 Fig. 10|Late Devonian|Late Devonian|Geological Province: Southern Carnarvon Basin.||||||
20073|Willaraddie Formation|60384|5|Briefly described|p244|Late Devonian|Late Devonian|Near eastern margin, Southern Carnarvon Basin. Described along with Munabia Sandstone as: coastal to nearshore sandstone with lesser claystone, conglomerate and dolomite.||||Probably lateral equivalent to Munabia Sandstone||
20073|Willaraddie Formation|61023|5|Briefly described|p34 Fig. 14|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
20073|Willaraddie Formation|61958|5|Briefly described|Map sheet 1|Devonian|Devonian|||||||
20073|Willaraddie Formation|64580|6|Mentioned|map legend|||Devonian succession, Southern Carnarvon Basin.||||||15-DEC-08
20073|Willaraddie Formation|67200|5|Briefly described|p7 fig 5,|Devonian|Devonian|||||Overlies Munabia Sandstone, overlain by Moogooree Limestone|Trough and planar cross bedded pebbly sandstone.|
20073|Willaraddie Formation|69011|5|Briefly described|Map Legend|Devonian|Devonian|Southern Carnarvon Basin.||||Overlain by the Moogooree Limestone. Underlain by the Munabia Sandstone.|Comprises poorly sorted, commonly pebbly, lithic sandstone, and granulte to pebble conglomerate; claystone.|
20073|Willaraddie Formation|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Early Carboniferous|Late Devonian|Carnarvon Basin. Deposited in an alluvial-fan environment. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Overlies the Munabia Sandstone.|Conglomerate and sandstone.|
20073|Willaraddie Formation|70138|5|Briefly described|Map legend.|Devonian|Devonian|Southern Carnarvon Basin.||||Overlies Munabia Sandstone. Is overlain by Moogooree Limestone.|Poorly sorted, commonly pebbly, lithic sandstone, and granule to pebble conglomerate; claystone.|
20073|Willaraddie Formation|70795|4|Described|100k_geologyp_lut.csv|Famennian|Famennian|Also 100k_interpgeop_lut.csv|372-359 Ma||||Poorly sorted, commonly pebbly, lithic sandstone, and granule to pebble conglomerate; claystone.|
20073|Willaraddie Formation|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|||||||
20073|Willaraddie Formation|71146|5|Briefly described|p6|Famennian|Famennian|Southern Carnarvon Basin.||||Overlies the Munabia Sandstone. Overlain by the Moogooree Limestone.|Sandstone.|
20073|Willaraddie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone, limestone|
20081|Williambury Formation|14228|5|Briefly described|p5 fig 2, p6 fig3, p7, p18|Visean|Tournaisian|Merlinleigh Sub-basin.||||Overlies Moogooree Limestone. Overlain by Yindagindy Formation.|Conglomerate, sandstone, siltstone of alluvial fan.|
20081|Williambury Formation|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
20081|Williambury Formation|23311|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|||||||
20081|Williambury Formation|23312|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|||||||
20081|Williambury Formation|23403|4|Described|p7|Early Carboniferous|Middle Devonian|Geological Province: Gascoyne Complex.||||||24-NOV-09
20081|Williambury Formation|23726|5|Briefly described|p29|Tournaisian|Tournaisian|Overlying unit Yindagindy Formation. Underlying unit Moogoree Limestone. Geological Province: Carnarvon Basin.||||||
20081|Williambury Formation|23815|4|Described|p277|Early Carboniferous|Early Carboniferous|Geological Province: Carnarvon Basin. Overlying units: Yindagindy Formation (conformable) and Lyons Group (unconformable). Underlying unit: Moogooree Limestone (conformable). Max. thickness: 338.||||||27-APR-05
20081|Williambury Formation|24059|5|Briefly described|p146|Early Carboniferous|Early Carboniferous|Geological Province: Carnarvon Basin.||||||
20081|Williambury Formation|24390|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
20081|Williambury Formation|30875|6|Mentioned|p10|||Carboniferous age||||||
20081|Williambury Formation|31561|5|Briefly described|p33|||See also P34. Early Carboniferous||||||
20081|Williambury Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
20081|Williambury Formation|32648|6|Mentioned|p32|||Tournaisian-Visean||||||
20081|Williambury Formation|32789|5|Briefly described|p82|||||||||
20081|Williambury Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
20081|Williambury Formation|33386|6|Mentioned|Fig.7|||||||||
20081|Williambury Formation|33453|5|Briefly described|p69|||||||||
20081|Williambury Formation|34085|6|Mentioned|Cor.chart|||Tourn-Visean||||||
20081|Williambury Formation|34846|6|Mentioned|Fig.3|||||||||
20081|Williambury Formation|35282|6|Mentioned|Fig.2|||||||||
20081|Williambury Formation|35981|6|Mentioned|p134|||||||||
20081|Williambury Formation|36257|6|Mentioned|Table 2.1|||||||||
20081|Williambury Formation|36890|3|Fully described|p277|||Formerly Williambury Sandstone.||||||15-DEC-08
20081|Williambury Formation|40617|6|Mentioned|p4|||Also Mention Fig.1||||||
20081|Williambury Formation|40992|6|Mentioned|Fig.8|||||||||
20081|Williambury Formation|41271|3|Fully described|p59|||Formerly "Williambury Sandstone".||||||15-DEC-08
20081|Williambury Formation|41438|6|Mentioned|p103|||||||||
20081|Williambury Formation|41443|6|Mentioned|p163|||||||||
20081|Williambury Formation|41444|6|Mentioned|Fig.4|||||||||
20081|Williambury Formation|41839|4|Described|p20|||Formerly "Williambury Sandstone"||||||
20081|Williambury Formation|42116|5|Briefly described|Fig.1 P5|||||||||
20081|Williambury Formation|42547|4|Described|p89|||||||||
20081|Williambury Formation|44344|14|Not recorded|p.6, opp.4, map||Carboniferous|(G50-1).||||||
20081|Williambury Formation|44345|14|Not recorded|map legend||Early Carboniferous|Lower Carboniferous.||||||
20081|Williambury Formation|44537|14|Not recorded|map legend|||? Upper Carboniferous.||||||
20081|Williambury Formation|44657|14|Not recorded|p.5,7,8|||||||||
20081|Williambury Formation|44994|5|Briefly described|p9|||Fig.6 Correlation.||||||
20081|Williambury Formation|45015|2|Defined|p67-72, map legend|Carboniferous|Carboniferous|Quartzwacke, conglomerate and pebbly quartzwacke. Conformably overlies Moogooree Limestone; conformably overlain by Yindagindy Formation; also unconformably overlain by Lyons Group units in places. Max. thickness: 1100ft. Geol. Prov: Carnarvon Basin.||||||31-MAY-06
20081|Williambury Formation|45016|14|Not recorded|p.9 (map)|||||||||
20081|Williambury Formation|45063|6|Mentioned|p30|||See also Fig. 9. Carb.||||||
20081|Williambury Formation|49942|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Geological Province: Merlinleigh Sun-basin.||||||
20081|Williambury Formation|50085|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
20081|Williambury Formation|60384|6|Mentioned|p244|Early Permian|Carboniferous|Merlinleigh Sub-Basin, Southern Carnarvon Basin. Alluvial fan.||||||
20081|Williambury Formation|61023|5|Briefly described|p34 Fig. 14|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
20081|Williambury Formation|61958|5|Briefly described|Map sheet 1|Early Carboniferous|Early Carboniferous|||||||
20081|Williambury Formation|64580|6|Mentioned|map legend|||Carboniferous succession, Southern Carnarvon Basin.||||||15-DEC-08
20081|Williambury Formation|64972|6|Mentioned|p614, p617 Fig. 5|Carboniferous|Carboniferous|||||||
20081|Williambury Formation|67200|5|Briefly described|p7 fig 5,|Carboniferous|Carboniferous|||||Overlain by Yindagindy Formation|Crudely bedded conglomerate.|
20081|Williambury Formation|69011|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlain by the Yindagindy Formation. Underlain by the Moogooree Limestone.|Comprises poorly sorted, silty, lithic sandstone, pebble to cobble conglomerate; claystone.|
20081|Williambury Formation|69182|5|Briefly described|Ch3 p8, Ch3 p10-p11|Early Carboniferous|Early Carboniferous|Carnarvon Basin. Deposited as part of an alluvial fan. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Overlies the Moogooree Limestone. Overlain by the Yindagindy Formation.|Conglomerate, sandstone and siltstone.|
20081|Williambury Formation|70138|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlies Moogooree Limestone. Is overlain by Yindagindy Formation.|Poorly sorted, silty lithic sandstone, pebble to cobble conglomerate; claystone.|
20081|Williambury Formation|70795|4|Described|100k_geologyp_lut.csv|Visean|Tournaisian|Also 100k_interpgeop_lut.csv|359-331 Ma||||Poorly sorted, silty lithic sandstone, siltstone and shale; pebble to cobble conglomerate in type section; poorly exposed.|
20081|Williambury Formation|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||||
20081|Williambury Formation|71146|5|Briefly described|p6, p34|Visean|Tournaisian|Southern Carnarvon Basin. Believed to be at least partially equivalent to the Anderson Formation and Weaber Group.||||Overlies the Moogooree Limestone. Overlain by the Yindagindy Formation.|Mudstone.|
20081|Williambury Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
20081|Williambury Formation|73117|6|Mentioned|p15|Visean|Visean|||||Overlain by Yindagindy Formation.||
20090|Williamstown Dolerite|22534|6|Mentioned|Fig.5 p10|||Of Kalgoorlie Group.||||||14-APR-08
20090|Williamstown Dolerite|23926|6|Mentioned|p19 Fig. 7|||||||||
20090|Williamstown Dolerite|23928|5|Briefly described|p66|Archean|Archean|Max. thickness: 350m. Geological Province: Yilgarn Craton.||||||07-NOV-08
20090|Williamstown Dolerite|29681|5|Briefly described|Table 2|||||||||
20090|Williamstown Dolerite|29784|6|Mentioned|Table 1|||||||||
20090|Williamstown Dolerite|30779|6|Mentioned|Table 1|||Stratigraphy||||||
20090|Williamstown Dolerite|30882|6|Mentioned|p50|||||||||
20090|Williamstown Dolerite|30886|6|Mentioned|Table 4|||||||||
20090|Williamstown Dolerite|30900|6|Mentioned|p67|||On Table 1.||||||
20090|Williamstown Dolerite|31042|6|Mentioned|Fig. 4|||Correlation||||||
20090|Williamstown Dolerite|32079|6|Mentioned|p435|||||||||
20090|Williamstown Dolerite|32083|6|Mentioned|p294|||||||||
20090|Williamstown Dolerite|32685|5|Briefly described|Table 1|||||||||
20090|Williamstown Dolerite|33515|6|Mentioned|p33|||||||||
20090|Williamstown Dolerite|33535|4|Described|p177|||||||||
20090|Williamstown Dolerite|34324|6|Mentioned|p122|||||||||
20090|Williamstown Dolerite|34608|6|Mentioned|p2|||||||||
20090|Williamstown Dolerite|35469|6|Mentioned|p44|||||||||
20090|Williamstown Dolerite|35611|6|Mentioned|Fig.2|||Stratigraphic columns for Kalgoorlie and Kambalda.||||||
20090|Williamstown Dolerite|36869|6|Mentioned|p48|||||||||
20090|Williamstown Dolerite|39046|6|Mentioned|Fig.2|||||||||
20090|Williamstown Dolerite|39895|5|Briefly described|Fig.1|||||||||
20090|Williamstown Dolerite|40005|6|Mentioned|Fig.16|||||||||
20090|Williamstown Dolerite|40083|6|Mentioned|Fig.2|||||||||
20090|Williamstown Dolerite|40849|4|Described|p49|||||||||
20090|Williamstown Dolerite|41066|6|Mentioned|1 of 2 L17|||||||||
20090|Williamstown Dolerite|41149|6|Mentioned|Fig.1|||||||||
20090|Williamstown Dolerite|41249|6|Mentioned|p4|||||||||
20090|Williamstown Dolerite|41458|6|Mentioned|p369|||||||||
20090|Williamstown Dolerite|41771|6|Mentioned|Fig.3|||||||||
20090|Williamstown Dolerite|41784|6|Mentioned|Table 1|||||||||
20090|Williamstown Dolerite|41889|6|Mentioned|Fig.1|||||||||
20090|Williamstown Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
20090|Williamstown Dolerite|42160|6|Mentioned|p45|||||||||
20090|Williamstown Dolerite|42195|6|Mentioned|Fig.4 P147|||||||||
20090|Williamstown Dolerite|42221|6|Mentioned|Table 1 P6|||||||||
20090|Williamstown Dolerite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
20090|Williamstown Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
20090|Williamstown Dolerite|42817|5|Briefly described|Fig.3|||||||||
20090|Williamstown Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
20090|Williamstown Dolerite|42892|6|Mentioned|p36|||||||||
20090|Williamstown Dolerite|42969|6|Mentioned|Fig.1 p106|||||||||
20090|Williamstown Dolerite|43162|6|Mentioned|5|||||||||
20090|Williamstown Dolerite|43496|5|Briefly described|12|||||||||03-MAR-10
20090|Williamstown Dolerite|44149|6|Mentioned|p88 fig 2-90|Archean|Archean|||||||
20090|Williamstown Dolerite|45546|14|Not recorded|p.50-52|||||||||
20090|Williamstown Dolerite|46905|5|Briefly described|Table 1|||Stratigraphic succession||||||
20090|Williamstown Dolerite|60514|6|Mentioned|p55 Fig. 2, p56 Fig. 3, p65 Table. 1|Archean|Archean|Of the Paringa Basalt (Kalgoorlie Group). Geological Province: Kambalda Domain Yilgarn Craton.||||||07-FEB-11
20090|Williamstown Dolerite|60626|6|Mentioned|p55 Fig.2|||||||||
20090|Williamstown Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Paringa Basalt.||||||
20090|Williamstown Dolerite|62108|5|Briefly described|p1409 Tb. 4|||Of the Kalgoorlie Group. Has in situ fractionation at base of Paringa Basalt which overlies it. Thickness: up to 300m. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1420 Fig. 14.||||||07-FEB-11
20090|Williamstown Dolerite|62109|5|Briefly described|p1429 Fig. 2|||||||||
20090|Williamstown Dolerite|62406|5|Briefly described|p54 Fig. 2, p55|||Relatively narrow heterogeneous mafic unit, comprising a serpentinite base with unaltered meta-basalt and irregularly altered mafics ranging from quartz gabbro through dolerite and basalt to devitrified andesite. Contains lode seams of Golden Mile type.||||||23-JUN-06
20090|Williamstown Dolerite|64016|6|Mentioned|p56|||Has a hornblendite base grading up into a pyroxene-rich gabbro.||||||
20090|Williamstown Dolerite|64715|5|Briefly described|p5 Fig. 4, p6|||Forms a sill. Local lithology details included. See also p7 Fig. 7||||||16-DEC-08
20090|Williamstown Dolerite|65204|6|Mentioned|pg6 Tbl.1, p12|Archean|Archean|Komatiitic and tholeiitic basalt; associated with Golden Mile Dolerite.||||||11-JUN-15
20090|Williamstown Dolerite|65834|6|Mentioned|p7, 12, 54, 56|||Kambalda Domain, Kalgoorlie Terrane.||Kalgoorlie Group.||||
20090|Williamstown Dolerite|68216|6|Mentioned|p301 Fig. 1|||SH51-9||||||
20090|Williamstown Dolerite|68217|4|Described|71-73, 75, 77-9|Precambrian|Precambrian|Approx 500 - 1000 ft thick [~150 - 300 m thick]||||Underlain by Kapai Slate. Overlain by Paringa Basalt.|Sill of meta-dolerite and meta-gabbro transitional to meta-quartz dolerite near top and hornblendite near base.|20-MAY-21
20090|Williamstown Dolerite|68289|6|Mentioned|p12-p13|||Mount Hunt-Hannan Lake area.|||||Peridotite altered to talc-tremolite-serpentine rock. Gabbro with pyroxene altered to tremolite and chlorite and plagioclase to chlorite.|
20090|Williamstown Dolerite|69035|5|Briefly described|pp413-416|||~ 250 m thick.|||||Consists of an olivine-bearing lower ultramafic section grading up into granophyric pyroxene gabbro.|
20090|Williamstown Dolerite|69619|6|Mentioned|p120|||Kalgoorlie area.||||Equivalent to Pernatty Dolerite.||
20090|Williamstown Dolerite|69631|5|Briefly described|p14-16|||Mount Hunt area.|||||A markedly differentiated sill, containing peridotite and gabbro; all primary minerals have been altered but are recognisable by preserved textures.|
20090|Williamstown Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2696 Ma (inferred).|Leviathan Suite|||Differentiated sill: basal pyroxenite to gabbro and quartz-bearing gabbro; minor granophyric phases in the upper section; metamorphosed.|
20090|Williamstown Dolerite|70287|6|Mentioned|p188|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.||||||
20090|Williamstown Dolerite|70326|5|Briefly described|p360,363|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. Age from granophyre, U-Pb SHRIMP (Fletcher et al., 2001).|2696+\-5 Ma (Fletcher et al., 2001).|||Intrudes into upper Paringa Basalt.||
20090|Williamstown Dolerite|70773|6|Mentioned|p22, p24 fig 16, p25 fig 18|||About 400m thick, this unit is poorly exposed and largely covered by talus.|||||Talc-tremolite-serpentine rock and altered gabbro.|
20090|Williamstown Dolerite|71166|6|Mentioned|p119 fig 3.89|||||||||
20090|Williamstown 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 gabbro and quartz-bearing gabbro; minor granophyric phases in the upper section; metamorphosed|
20090|Williamstown Dolerite|72049|5|Briefly described|p253, p258-p259, p267-p268|Neoarchean|Neoarchean|Affinities with the Powder Sill Gabbro and the Vivien Dolerite. Occurs near Kalgoorlie.|2696 +/- 5 Ma (SHRIMP U-Pb)|||Intrudes the Kambalda Sequence.||
20090|Williamstown Dolerite|72095|5|Briefly described|p10-11, 14-17,20, 21|||Kalgoorlie Region, Eastern Goldfields, Yilgarn Craton. Detailed geochemistry is described.||||||
20090|Williamstown Dolerite|73300|6|Mentioned|p1112-1113|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie terrane.|2696 +/- 5 Ma||||Dolerite sill, intrudes volcano-sedimentary sequence.|
20090|Williamstown Dolerite|73391|5|Briefly described|p114, 206, 308, Appendices.|||Woodall (1965). Kalgoorlie area.||Upper Basalt.|||Dolerite-gabbro sill with lower ultramafic rocks.|
20155|Wilson Bluff Limestone|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|22613|5|Briefly described|p21|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|22614|5|Briefly described|map|Eocene|Eocene|||||||
20155|Wilson Bluff Limestone|22626|4|Described|437-439|Late Eocene|Middle Eocene|Geol province Eucla Basin. Max thickness 300 m||||||
20155|Wilson Bluff Limestone|22814|5|Briefly described|p258, fig2|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|23331|4|Described|1089|Late Eocene|Middle Eocene|||||||10-SEP-09
20155|Wilson Bluff Limestone|23488|5|Briefly described|p36, p38 Fig. 3|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|23533|6|Mentioned|p560|||See also p564 Fig 3.||||||
20155|Wilson Bluff Limestone|23584|6|Mentioned|p29|||Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|23671|6|Mentioned|p1|||Disconformably overlies the Pidinga Formation.||||||
20155|Wilson Bluff Limestone|23768|5|Briefly described|p28 Fig. 5|Eocene|Eocene|Geological Province: Eucla Basin.  See also p39, p79.||||||
20155|Wilson Bluff Limestone|23818|4|Described|p174 Fig.84, p196, 198|Late Eocene|Middle Eocene|Geological Province: Eucla Basin. Max. thickness: 400 ft. Overlying unit: Nullarbor Limestone.||||||
20155|Wilson Bluff Limestone|23989|5|Briefly described|p54 Fig. 46|Late Eocene|Middle Eocene|Overlies Yilgarn Craton||||||04-NOV-10
20155|Wilson Bluff Limestone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24094|4|Described|p272|Middle Eocene|Early Eocene|See also Wilson Bluff Limestone Formation. Li et al (1996) suggests the type section for Wilsons Bluff Limestone actually belongs to Abrakurrie Limestone. Geological Province: Eucla Basin||||||16-MAR-05
20155|Wilson Bluff Limestone|24201|5|Briefly described|p373 Fig. 2|Oligocene|Eocene|||||||
20155|Wilson Bluff Limestone|24338|5|Briefly described|p938 Fig. 2|Rupelian|Lutetian|Overlies the Pidinga Formation. Geological Province: Bight Basin.||||||
20155|Wilson Bluff Limestone|24347|5|Briefly described|p114|Late Eocene|Middle Eocene|Underlying unit: Hampton Sandstone.  Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24350|5|Briefly described|Fig. 4 Appdx|Oligocene|Eocene|Part of the Dugong Supersequence.||||||
20155|Wilson Bluff Limestone|24396|5|Briefly described|p222|Eocene|Eocene|Formerly contained the Paling Member (of Alley and Beecroft, 1993) however this member has now been raised to Paling Formation.  Overlies Gawler Craton.||||||04-NOV-10
20155|Wilson Bluff Limestone|24397|4|Described|p237-238|Eocene|Eocene|Formerly Wilson's Bluff Limestone (Singleton, 1954).  Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|24443|5|Briefly described|Fig.7|Oligocene|Eocene|Overlies Piginda Formation. Geological Province: Bight Basin.||||||
20155|Wilson Bluff Limestone|24553|5|Briefly described|Figs. 7,8 and 10|Late Eocene|Middle Eocene|Along with Nullarbor Limestone, shown as equivalent to the Dugong Supersequence.||||||21-JAN-16
20155|Wilson Bluff Limestone|24557|5|Briefly described|p958, p959, p960 Fig.3|Late Eocene|Late Eocene|Offshore marine sediments: limestone and marl; biota dominated by bryozoans, with moderate foraminifera, echinoids, and locally abundant serpulids. Geological Province: Bremer Basin.||||||11-JAN-05
20155|Wilson Bluff Limestone|24606|5|Briefly described|p956|Late Eocene|Middle Eocene|Conformably overlies the Hampton Sandstone. Geological Province: Eucla Basin||||||
20155|Wilson Bluff Limestone|24617|6|Mentioned|p113, p115 Fig. 3|Eocene|Eocene|Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|29591|5|Briefly described|p92|||||||||
20155|Wilson Bluff Limestone|29601|6|Mentioned|p82|||Upper Eocene||||||
20155|Wilson Bluff Limestone|29856|6|Mentioned|p37|||||||||
20155|Wilson Bluff Limestone|30012|4|Described|Table 1|||||||||
20155|Wilson Bluff Limestone|30230|6|Mentioned|p32|||Eocene age.||||||
20155|Wilson Bluff Limestone|30515|6|Mentioned|p69|||||||||
20155|Wilson Bluff Limestone|30563|4|Described|p12|||On Stratigraphic table||||||
20155|Wilson Bluff Limestone|30564|5|Briefly described|p4|||||||||
20155|Wilson Bluff Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20155|Wilson Bluff Limestone|30828|6|Mentioned|p113|||||||||
20155|Wilson Bluff Limestone|30917|6|Mentioned|p53|||||||||
20155|Wilson Bluff Limestone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
20155|Wilson Bluff Limestone|30945|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|30975|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
20155|Wilson Bluff Limestone|31049|6|Mentioned|p394|||||||||
20155|Wilson Bluff Limestone|31051|6|Mentioned|p.83.|||||||||
20155|Wilson Bluff Limestone|31053|6|Mentioned|p545|||||||||
20155|Wilson Bluff Limestone|31318|5|Briefly described|p166|||U. Eocene||||||
20155|Wilson Bluff Limestone|31562|5|Briefly described|p13|||||||||
20155|Wilson Bluff Limestone|31847|6|Mentioned|p49|||Correlation||||||
20155|Wilson Bluff Limestone|31850|4|Described|p33|||Summary of definition||||||
20155|Wilson Bluff Limestone|31902|4|Described|Table 1|||Fig.1||||||
20155|Wilson Bluff Limestone|31903|6|Mentioned|Map legend|Tertiary|Tertiary|Section only||||||
20155|Wilson Bluff Limestone|31904|4|Described|p7|||See Table 1. Refers previous authors.||||||
20155|Wilson Bluff Limestone|31906|4|Described|p7|||See Table 1. Refers previous authors.||||||
20155|Wilson Bluff Limestone|31907|3|Fully described|p7|||See also Table 1, Fig.1||||||
20155|Wilson Bluff Limestone|31908|4|Described|Table 1|||U.-M. Eocene||||||
20155|Wilson Bluff Limestone|31909|3|Fully described|p7|||||||||
20155|Wilson Bluff Limestone|31913|4|Described|p10|||Table 1||||||
20155|Wilson Bluff Limestone|31915|6|Mentioned|Map legend|Eocene|Eocene|||||||
20155|Wilson Bluff Limestone|31923|6|Mentioned|p18|||||||||
20155|Wilson Bluff Limestone|32117|6|Mentioned|Fig.2|||||||||
20155|Wilson Bluff Limestone|32120|6|Mentioned|p276|||Eocene fauna||||||
20155|Wilson Bluff Limestone|32552|2|Defined|p10|late Eocene|middle Eocene|Mid.-U.Eocene. See also P27, 37, 53, 54 etc.M - U||||||
20155|Wilson Bluff Limestone|32648|6|Mentioned|p32|||U.Eocene||||||
20155|Wilson Bluff Limestone|32750|6|Mentioned|p304|||Stratigraphy||||||
20155|Wilson Bluff Limestone|33586|4|Described|Table 1|||See also P14.||||||
20155|Wilson Bluff Limestone|33589|4|Described|p11|||U. Eocene.||||||
20155|Wilson Bluff Limestone|33595|6|Mentioned|p6|||||||||
20155|Wilson Bluff Limestone|34180|6|Mentioned|p229|||Tertiary||||||
20155|Wilson Bluff Limestone|34192|6|Mentioned|Map legend|Oligocene|Eocene|Lower Miocene - Eocene||||||
20155|Wilson Bluff Limestone|34194|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20155|Wilson Bluff Limestone|34232|6|Mentioned|p76|||Cavities.||||||
20155|Wilson Bluff Limestone|34287|6|Mentioned|p200|||||||||
20155|Wilson Bluff Limestone|34308|4|Described|p196|||M.- U.Eocene. Cor. chart Fig.84||||||
20155|Wilson Bluff Limestone|34344|6|Mentioned|p3|||Middle Eocene.||||||
20155|Wilson Bluff Limestone|34615|6|Mentioned|p10|||||||||
20155|Wilson Bluff Limestone|34742|6|Mentioned|Map legend|late Eocene|late Eocene|||||||
20155|Wilson Bluff Limestone|34759|6|Mentioned|p60|||||||||
20155|Wilson Bluff Limestone|35051|6|Mentioned|p204|||||||||
20155|Wilson Bluff Limestone|35097|6|Mentioned|p16|||||||||
20155|Wilson Bluff Limestone|35496|4|Described|Table 1|||Also on p21.||||||13-SEP-18
20155|Wilson Bluff Limestone|35772|6|Mentioned|Table 1|||See also p11.||||||13-SEP-18
20155|Wilson Bluff Limestone|36200|6|Mentioned|Table 1|||||||||
20155|Wilson Bluff Limestone|36257|6|Mentioned|Table 2.1|||||||||
20155|Wilson Bluff Limestone|36890|3|Fully described|p413|||Formerly Wilsons Bluff Limestone||||||
20155|Wilson Bluff Limestone|36915|6|Mentioned|Fig.7|||||||||
20155|Wilson Bluff Limestone|37852|6|Mentioned|p5|||||||||
20155|Wilson Bluff Limestone|38068|6|Mentioned|Fig.7|||||||||
20155|Wilson Bluff Limestone|38553|6|Mentioned|p41|||||||||
20155|Wilson Bluff Limestone|38602|6|Mentioned|p2|||||||||
20155|Wilson Bluff Limestone|38773|6|Mentioned|p46|||||||||
20155|Wilson Bluff Limestone|39173|6|Mentioned|p325|||||||||
20155|Wilson Bluff Limestone|39923|6|Mentioned|p354|||||||||
20155|Wilson Bluff Limestone|40003|5|Briefly described|Table 14|||See also Fig.16 and P54||||||
20155|Wilson Bluff Limestone|40298|6|Mentioned|p433|||||||||
20155|Wilson Bluff Limestone|40410|6|Mentioned|p4|||||||||
20155|Wilson Bluff Limestone|40421|6|Mentioned|p60|||||||||
20155|Wilson Bluff Limestone|40429|6|Mentioned|p26|||||||||
20155|Wilson Bluff Limestone|40992|6|Mentioned|Fig.23|||||||||
20155|Wilson Bluff Limestone|41043|6|Mentioned|p87|||||||||
20155|Wilson Bluff Limestone|41076|6|Mentioned|p70|||||||||
20155|Wilson Bluff Limestone|41517|6|Mentioned|p139|||||||||
20155|Wilson Bluff Limestone|41626|6|Mentioned|p48|||||||||
20155|Wilson Bluff Limestone|42086|5|Briefly described|Fig.2 P4|||||||||
20155|Wilson Bluff Limestone|42108|4|Described|p321|||See also Fig.1||||||
20155|Wilson Bluff Limestone|42335|4|Described|p325|||||||||
20155|Wilson Bluff Limestone|42356|5|Briefly described|Fig.15 P119|late Eocene|middle Eocene|See also Microfiche 7 p15, Fig.4, Fig.9, 10, 12, 13.||||||
20155|Wilson Bluff Limestone|42428|5|Briefly described|p1006|||||||||
20155|Wilson Bluff Limestone|42734|5|Briefly described|map legend|Tertiary||||||||
20155|Wilson Bluff Limestone|42816|5|Briefly described|p23|||||||||
20155|Wilson Bluff Limestone|42862|5|Briefly described|p8|||||||||
20155|Wilson Bluff Limestone|42959|5|Briefly described|p58 Fig.3|||||||||
20155|Wilson Bluff Limestone|43026|6|Mentioned|p589|||||||||
20155|Wilson Bluff Limestone|43040|5|Briefly described|Fig.2,p861|||||||||
20155|Wilson Bluff Limestone|43049|5|Briefly described|p23|||||||||
20155|Wilson Bluff Limestone|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|||||||
20155|Wilson Bluff Limestone|43498|6|Mentioned|8||Late Eocene|||||||
20155|Wilson Bluff Limestone|43658|6|Mentioned|p5||Eocene|||||||
20155|Wilson Bluff Limestone|43672|5|Briefly described|p330|||||||||
20155|Wilson Bluff Limestone|43813|6|Mentioned|p133|||||||||
20155|Wilson Bluff Limestone|43814|6|Mentioned|Fig.3,p115|||||||||
20155|Wilson Bluff Limestone|44133|4|Described|p182|Early Oligocene|Middle Eocene|Geological Province: Eucla Basin. Conformably overlies: Pidinga Formation and Hampton Sandstone. Thickness: ~300m. Intertongues and underlies Toolinna Limestone. Underlies Abrakurrie and Nullarbor Limestones.||||||11-JUL-13
20155|Wilson Bluff Limestone|44145|4|Described|p551 Tbl 4-27, p555-6, fig 4-194,|Late Eocene|Middle Eocene|Eucla Basin. Thickness up to 300m known. Rich and varied fauna.||||Disconformably overlies Madura Formation. Overlies and grades laterally into Hampton Sandstone. Upper part grades laterally into Toolinna Limestone. Unconformably overlain by Abracurrie Limestone.|Chalky bryozoan calcarenite packstone with chert nodules. Basal glauconitic marl in places.|
20155|Wilson Bluff Limestone|44412|14|Not recorded|map legend||Eocene|Middle to Upper Eocene.||||||
20155|Wilson Bluff Limestone|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
20155|Wilson Bluff Limestone|44864|5|Briefly described|Map Legend||Miocene|||||||
20155|Wilson Bluff Limestone|45149|4|Described|p62|||See also p60.||||||13-SEP-18
20155|Wilson Bluff Limestone|45168|6|Mentioned|Table 1 P6|||||||||
20155|Wilson Bluff Limestone|47054|6|Mentioned|p490|||||||||
20155|Wilson Bluff Limestone|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Includes bryozoan clacarenites. Overlies and interfingers with Hampton Sandstone; overlain by and interfingers with Toolinna Limestone. Age: 44-38.5Ma. Max. thickness: 300m. Geological Province: Eucla Basin and the Great Australian Bight.||||||
20155|Wilson Bluff Limestone|61197|5|Briefly described|p473, p475, p478 Fig.4, p488|Late Eocene|Middle Eocene|Eucla Basin. Marine deep-shelf deposits. 0-40m thick.|||||Chalky, bryozoan calcarenite; common chert nodules; minor glauconite.|
20155|Wilson Bluff Limestone|61517|5|Briefly described|p309|Eocene|Eocene|Unconformably overlain by Roe Calcarenite. Geological Province: Eucla Basin.||||||
20155|Wilson Bluff Limestone|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|||||Overlies Pidinga Formation.||
20155|Wilson Bluff Limestone|61630|6|Mentioned|p555 Fig. 3|Oligocene|Eocene|Geological Province: Eyre Sub-basin, Bright and Duntroon Basins. Marine.||||||07-APR-09
20155|Wilson Bluff Limestone|61856|5|Briefly described|p300 Fig.2, p304, p311, p314-317 |Eocene|Eocene|Thickness: up to 300m.||||Conformably overlies Hampton Sandstone.|Thick marine limestone; sandy and glauconitic in the lower part.|23-JAN-15
20155|Wilson Bluff Limestone|62369|5|Briefly described|p409, p410 Fig.4|Late Eocene|Middle Eocene|White, muddy, burrowed unit, rich in bryozoans and planktonic foraminifers. Overlies Hampton Sandstone. Thickness: ~300m. Geological Province: Eucla Basin.||||||04-NOV-10
20155|Wilson Bluff Limestone|62640|5|Briefly described|p65, pp67-77.       |Late Eocene|Middle Eocene|Oldest and thickest limestone of the Eucla Basin; up to 300m thick. High porosity, low permeability.|c.42 - c.37 Ma.|||Overlies Madura Formation. Intertongues with the Toolinna Limestone in the southwest of the Eucla Basin. Is overlain by Abrakurrie Limestone.|Predominantly sand-sized fragments of calcareous skeletons in a very fine-grained calcite matrix.|
20155|Wilson Bluff Limestone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Oligocene|Late Eocene|Geological Province: Eucla Basin.||||||08-FEB-10
20155|Wilson Bluff Limestone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Age shown as Lutetian to Priabonian.||||||
20155|Wilson Bluff Limestone|65942|2|Defined|p77-78||Miocene|||Of Eucla Group.||||
20155|Wilson Bluff Limestone|66131|6|Mentioned|p242 Fig.2|Eocene|Eocene|Middle to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
20155|Wilson Bluff Limestone|67117|5|Briefly described|Map legend.|Miocene|Eocene|Shown under general heading of 'Eocene - Miocene'.|||||White to grey wackestone; skeletal mudstone, rudstone and minor packstone; locally laminations and scour channels, infilled with coarser material.|03-MAY-13
20155|Wilson Bluff Limestone|67462|5|Briefly described|Map legend.|Eocene|Eocene|Bunda Plateau, Eucla Basin.||||||
20155|Wilson Bluff Limestone|67789|5|Briefly described|p34-35, 39-40, 45-46|Eocene|Eocene|Eucla Basin. Up to 300m thick. Contains the best developed deep caves in the Nullarbor Plain.||Eucla Group.||Is overlain by Abrakurrie Limestone.|A soft, poorly lithified, muddy to chalky bryozoan-rich cool-water carbonate.|
20155|Wilson Bluff Limestone|68715|6|Mentioned|p30 Fig.5|Priabonian|Lutetian|Bunda Plateau, Eucla Basin.||||||23-JAN-15
20155|Wilson Bluff Limestone|69004|5|Briefly described|p19, p34|Upper Eocene|Middle Eocene|Eucla Basin. Informally subdivided into an upper and lower part.|||||Carbonates including limestone.|
20155|Wilson Bluff Limestone|69598|5|Briefly described|p2, p9, p11 Tb.1, p29 Tb.4|||Eucla Basin. Up to 300m thick. Potential carbon dioxide storage reservoir.|||||Fine-grained to chalky limestone that is commonly rich in bryozoans and echinoids.|
20155|Wilson Bluff Limestone|69648|4|Described|p4, p22-24, map legend|Eocene|Eocene|Eucla Basin. Temperate water, bryozoan limestones form foundation of a carbonate platform. First recognised by Tate (1879), who referred to it as the 'white polyzoal limestone'. Forms lower white band of cliffs that front the Great Australian Bight. Was deposited on a very broad (i.e. ~1000 km wide) and gently inclined platform, or a ramp where the higher energy facies predominate near the shore. The generally muddy nature of sediments indicate deposition mostly below fairweather wavebase. Age: Middle to Late Eocene (modified to early Late Eocene by Alley and Beecroft, 1993); significantly eroded during Oligocene to Early Miocene. Thickness: >50 m in SW OOLDEA and increases toward platform margin to ~300 m.||Eucla Group|Paling Member|Conformably overlies, and interfingers with, Pidinga Formation and Hampton Sandstone.|Marine platform bioclastic carbonates; dominantly muddy or micritic, bryozoan limestone; skeletal mudstone, wackestone (dominant), packstone and grainstone, and rudstone textures; lower/basal part can be glauconitic.|
20155|Wilson Bluff Limestone|69649|6|Mentioned|p31,|Eocene|Eocene|Eucla Basin.||||||
20155|Wilson Bluff Limestone|70397|5|Briefly described|p1-3|Late Eocene|Middle Eocene|Eucla Basin. Depositional environment: cool-temperate, open-marine shelf.||Unit of Eucla Group.||Unconformabyl overlain by Abrakurrie Limestone. Underlain by Hampton Sandstone.|Fine- to medium-grained bryozoan and planktonic foraminifera facies.|29-JUL-19
20155|Wilson Bluff Limestone|70722|5|Briefly described|p227-228|Eocene|Eocene|Of St. Vincent Basin. Lithologically different from Kangaroo Island late Eocene limestones, and areal distribution confirms a strong shelf partitioning, inboard biosiliceous and outboard carbonate (Gammon et al., 2003).|||||Fine-grained bryozoan-rich chalky limestones.|
20155|Wilson Bluff Limestone|70771|4|Described|p3, p7-p8, p27, p53-p58, p60-p61|Late Eocene|Middle Eocene|Eucla Platform, Eucla Basin. Commonly fossiliferous including abundant bryozoans, echinoids, bivalves, brachiopods and foraminifers. Extends to the inner margin of the Eucla Platform attaining a maximum thickness of approximately 300m. Interpreted to have been deposited on a cool to temperate continental shelf in water depths of 90-120m. [The author assigns this unit to the Eucla Group however this term is obsolete].||Eucla Group||Overlies the Hampton Sandstone. Disconformably overlain by the Abrakurrie Limestone and the Roe Calcarenite.|White, poorly-sorted chalky and fossiliferous limestone.|
20155|Wilson Bluff Limestone|70778|5|Briefly described|p4, p10|||Intersected in Nundroo 3 DDH.|||||Calcareous mudstone and glauconite.|
20155|Wilson Bluff Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke|
20155|Wilson Bluff Limestone|71361|4|Described|p5, p12, p15-p18, p23, p120|Late Eocene|Middle Eocene|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 to temperate deep shelf with water up to 300m deep. This unit contains abundant bryozoan and planktonic foraminifera fossils.||Eucla Group||Overlies the Hampton Sandstone. Unconformably overlain by the Abrakurrie Limestone and the Nullarbor Limestone.|Fine-grained bryozoan limestone, wackestone, packstone, chalky mudstones and grainstones.|
20155|Wilson Bluff Limestone|71789|14|Not recorded|p101|||Equivalent to Pallinup Siltstone.||||||
20155|Wilson Bluff Limestone|72344|5|Briefly described|p5, p16, p49, p61|||Eucla Basin. <150m thick east of the Coompana Block, increasing westwards to up to 300m thick in WA. Interpreted to have been deposited in a marine transgression on a drowned carbonate platform. See also p84, p96, p160, p169.||||Overlies the Hampton Sandstone. Overlain by the Abrakurrie Limestone.|Wackestone, white to grey, skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels infilled with coarser material.|
20155|Wilson Bluff Limestone|72465|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. <150m thick E of the Coompana Block, increasing westwards to 300m thick in WA. Forms the whitish cross-bedded and parallel-bedded unit in the lower Bunda Cliffs.||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudestone and minor packstone. Local laminations and minor scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72466|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Benbow et al. (1995). Eucla Basin, Coompana Province. <150m thick east of the Coompana Block, thickening westwards to 300m thick in WA. Deposited during marine transgressions on a drowned carbonate platform. Forms whitish cross-bedded and parallel-bedded unit in lower parts of the Bunda Cliffs. Also appears as Wilson's Bluff Limestone on p14 and as Wilsons Bluff limestone on p15.||||Overlies Hampton Sandstone and Pidinga Formation. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey, skeletal mudstone, rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72467|5|Briefly described|p9, 14-15, 17|Tertiary|Tertiary|Eucla Basin, Coompana Province. <150m thick E of the Coompana Block, increasing westwards to 300m thick in WA. Forms the whitish cross-bedded and parallel-bedded unit in the lower Bunda Cliffs. Also appears as Wilson's Bluff Limestone (p14) and Wilsons Bluff Limestone (p15).||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudestone and minor packstone. Local laminations and minor scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72468|5|Briefly described|p9, p14-15, p17|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72469|5|Briefly described|p9, p14-15, p17|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72470|5|Briefly described|p9, p14-15, p18|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72471|5|Briefly described|p9, p15, p17|||Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|72472|5|Briefly described|p9, p14-15|||[Also written as Wilson's Bluff Limestone]. Eucla Basin. Less than 150 m thick in the east, thickening to c. 300 m in the west. Deposited during marine transgression on a drowned carbonate platform. Forms the whitish cross-bedded and parallel-bedded unit in the lower parts of the Bunda Cliffs. Hosts an unconfined aquifer.||||Underlain by Hampton Sandstone. Overlain by Abrakurrie Limestone.|Wackestone, white to grey; skeletal mudstone; rudstone and minor packstone. Locally laminations and scour channels, infilled with coarser material.|
20155|Wilson Bluff Limestone|73084|5|Briefly described|p16-17|Eocene|Eocene|Eucla Basin.||||Underlain by Hampton Sandstone. Overlain by Nullarbor Limestone.|Chalky, fossiliferous limestone.|
20155|Wilson Bluff Limestone|73112|5|Briefly described|Map legend.|Eocene|Eocene||||||White bryozoal chalk with flints.|
20155|Wilson Bluff Limestone|73641|5|Briefly described|p5|Eocene|Eocene|Eucla Basin. 150 to ~300m thick. Deposited during a marine transgression on a drowned carbonate platform.||||Overlies Hampton Sandstone. Is overlain by Abrakurrie Limestone.|White to grey skeletal mudstone, rudstone and minor packstone. Local laminations and scour channels infilled with coarser material.|
20191|Winburn Granite|30385|4|Described|p13|||||||||
20191|Winburn Granite|30386|5|Briefly described|p13|||||||||
20191|Winburn Granite|30388|6|Mentioned|p15|||See also P19||||||
20191|Winburn Granite|30390|4|Described|p94|||||||||
20191|Winburn Granite|36886|4|Described|p201|||||||||
20191|Winburn Granite|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Winburn Suite.||||||
20191|Winburn Granite|67375|5|Briefly described|p20 Fig.11, p39, pp41-42. |Mesoproterozoic|Mesoproterozoic|Palgrave area, Talbot Sub-basin.|1077 +/- 6 Ma to 1055 +/- 10 Ma.|||Intrudes Mount Palgrave Group.|Fine- to medium-grained, equigranular to porphyritic, typically rapakivi-textured, moinzogranite to alkali-feldspar granite and quartz alkali feldspar syenite; mafics include biotite, blue-green amphibole and clinopyroxene.|
20191|Winburn Granite|67553|5|Briefly described|p41-44,84,93,95|||Geological province: Musgrave Province, North Australian Craton. Crystallisation ages range for variosu phases of the Winburn Granite, ranging from 1077+\-6 Ma (GSWA 174662) for a sample from Eliza Rocks, containing inclusions of an older granite phase,||||Intrudes into, and underlain by Mount Palgrave Group.|Fine- to medium-grained, from equigranular to porphyritic (and typically rapakivi-textured), and from monzogranitic to alkali-feldspar granite and quartz alkali feldspar syenite.|
20191|Winburn Granite|68995|5|Briefly described|p7-8, p10, p24-27, p35 Fig.20, p45, p57 |||Misspelt several times as the Winburn granite. See also p61-63.||||Overlain by (or intrudes) the Eliza Formation and the Mount Palgrave Group.|Fine-medium grained, equigranular to porphyritic (and rapakivi textured) granites that range from syenogranitic to alkali-feldspar granite to quartz-alkali-feldspar syenite.|
20191|Winburn Granite|69003|5|Briefly described|p50-52|Mesoproterozoic|Mesoproterozoic|Palgrave area, Talbot Sub-basin.|1077 +/- 6 Ma.|||Intrudes or is overlain by Mount Palgrave and Kaarnka Groups.||
20191|Winburn Granite|69091|4|Described|p71 Fig.4.14, p74-6, see comments|||A large, composite, synvolcanic intrusion that underlies and intrudes lowermost preserved rhyolitic unit of Talbot Sub-basin, and outcrops extensively along uplifted eastern and northern part of the sub-basin. Many granite phases can be matched geochemically with various rhyolitic units of Talbot Sub-basin. Misspelled as Winburn granite on p80, p84, p85 and p206. See also p80, p84-5, p103 Fig.5.6, p106 Fig.5.7a, p107 Fig.5.8a, p109 Fig.5.10, p114, p115 Fig.5.14, p116, p117 Fig.5.15, p127, p205.|1077 +/- 6 Ma|Warakurna Supersuite||Intrudes, or is overlain by, Mount Palgrave Group.|Large, composite, synvolcanic intrusion; granite.|
20191|Winburn Granite|69153|6|Mentioned|Rocks.csv||||||||Sample description: dark purplish-grey; fine-grained (crystal size about 1-2 mm); equigranular; massive (micro-)granite. Feldspar mainly subhedral; quartz anhedral. Rock looks feldspar-rich. Granophyre.|
20191|Winburn Granite|69655|5|Briefly described|p30, p66|||Strongly ferroan and alkaline-calcic (A-type) derived through fractionation of mantle derived mafic magmas.|||||A-type granite.|
20191|Winburn Granite|69729|5|Briefly described|p80, p82|||Syn-volcanic (and sub-volcanic) intrusion in the Talbot Sub-basin. Appears as Winburn granite on p82.||||Intrudes the Mount Palgrave Group (Bentley Supergroup).||
20191|Winburn Granite|70095|5|Briefly described|p16-17,19,21|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Intruded into, and removed the base of Mount Palgrave Group. Dolerites make up 30% of the volume of the Winburn Granite. See p19 Table 2 for U-Pb zircon data. See p21 Table 3 for SIMS oxygen isotope data.||||Overlain by Eliza Formation/Mount Palgrave Group. Underlain by Giles intrusions or Kunmarnara Group.||
20191|Winburn Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granophyre, aplite, granite|
20191|Winburn Granite|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Winburn Suite.|||Granite, granophyre, marginal porphyritic granophyre and aplite also forms apophyses into Palgrave Volcanic Association rocks and into the Pussy Cat Group|
20191|Winburn Granite|72443|6|Mentioned|p738-739, p742, p753||||1059 +/- 20 Ma to 1074 +/- 8 Ma (SHRIMP U-Pb)|Warakurna Supersuite||||
20198|Windalia Radiolarite|6876|6|Mentioned|p100 Fig.5.|Cretaceous|Cretaceous|||||||
20198|Windalia Radiolarite|12471|6|Mentioned|p475 Fig.2. |Early Cretaceous|Early Cretaceous|See also Figs 3, 4.||Unit in Winning Group.||Overlies Muderong Shale. Is overlain by Gearle Siltstone.||27-OCT-14
20198|Windalia Radiolarite|12491|5|Briefly described|pp459-462.|||Low permeability siltstones saturated by gas, sealed by Gearle Siltstone. Shows a strong seismic amplitude anomaly.||||Overlies Muderong Shale. Is overlain by Gearle Siltstone.||
20198|Windalia Radiolarite|12729|5|Briefly described|p.15, 17||Cretaceous|Prominent sequence boundary at the top of this unit. Deposited in a low-energy, marine environment with relatively low clastic-material input.||Winning Group||Overlies the Muderong Shale, underlies the Gearle Siltstone and Alinga Formation.||
20198|Windalia Radiolarite|13354|6|Mentioned|p386.|Late Cretaceous|Early Cretaceous|Carnarvon Basin.||16||||28-OCT-14
20198|Windalia Radiolarite|13615|3|Fully described|p4-p5, p6-p8, p18-p19|Albian|Aptian|Peedamullah Shelf. Up to 190m thick. Spores/Pollen Zone and Dinoflagellate zones provided. Small gas accumulations imaged in this unit. This unit together with the Muderong Shale forms the best potential Cretaceous source rocks in the Peedamullah Shelf. Type section found on Windalia Hill, Winning Station; 23deg16'10"S 114deg47'10E. Contains rich fauna of common radiolarians, ammonites, belemnites and foraminifers. Deposited in a shallow marine shelf environment. Permeability detailed. See also p35-p36, p38-p39, p42, p51-p52, p56, p58-p59, p63, p67, p72, p81, p83, p101 App.3, p118, Plates 2, 3.||Winning Group||Conformably overlies the Windalia Sandstone Member (Muderong Shale). Conformably overlain by the Gearle Siltstone.|Glauconitic, radiolarian siltstone and calcilutite; minor argillaceous sandstone, chert and calcareous claystone to marl.|12-FEB-19
20198|Windalia Radiolarite|14228|5|Briefly described|p5 Fig.2, p9, p26|Aptian|Aptian|||Winning Group||Overlies Muderong Shale. Overlain by Gearle Siltstone.|Dark grey siltstone, hard; bedded chert.|
20198|Windalia Radiolarite|23311|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group.||||||
20198|Windalia Radiolarite|23312|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Winning Group.||||||
20198|Windalia Radiolarite|23355|5|Briefly described|8 Fig.1|Early Cretaceous|Early Cretaceous|||||||
20198|Windalia Radiolarite|23379|5|Briefly described|p160 Fig.2; p162,164,167,168,171-174||Albian|Of Barrow Sub-basin.||||||07-NOV-06
20198|Windalia Radiolarite|23403|4|Described|p9|Late Cretaceous|Early Cretaceous|Of Winning Group.||||||24-NOV-09
20198|Windalia Radiolarite|23535|5|Briefly described|p125 Fig 3||Aptian|||||||
20198|Windalia Radiolarite|23572|4|Described|p11|Early Cretaceous|Early Cretaceous|Name appears to be used interchangeably with Windalia Sandstone Member. Geological Province: Carnarvon Basin. Of the Wininning Group. Underlying Unit: Muderong Shale. Overlying Unit: Gearle Siltstone and Alinga Formation.||||||16-MAY-05
20198|Windalia Radiolarite|23585|6|Mentioned|p25|||||||||
20198|Windalia Radiolarite|23726|5|Briefly described|p26|||Underlain by Muderong Shale. Geological Province: Carnarvon Basin.||||||07-NOV-06
20198|Windalia Radiolarite|23757|6|Mentioned|p17|||Ammonite sp. found.  Geological province: Carnarvon Basin.||||||
20198|Windalia Radiolarite|23815|4|Described|p297|Aptian|Aptian|Geological Province: Carnarvon Basin. Overlain by Gearle Siltstone and Alinga Formation (conformable). Underlain by Muderong Shale and Birdrong Sandstone (conformable). Max. thickness: 123 m. Fossiliferous.||||||07-NOV-06
20198|Windalia Radiolarite|23915|5|Briefly described|p518 Table 1|Cretaceous|Cretaceous|Disconformably underlies Gearle Siltstone.  Geological province: Southern Carnarvon Basin.||||||07-NOV-06
20198|Windalia Radiolarite|23935|4|Described|p11 Fig.7, p12 Fig.8|Albian|Aptian|Of Winning Group. Disconformably overlies Muderong Shale. Disconformably overlain by Gearle Siltstone. Dark grey to black siliceous siltstone. Thickness: 28 m. Geological Province: Southern Carnarvon Basin.||||||
20198|Windalia Radiolarite|23978|5|Briefly described|Map Legend|||||||||
20198|Windalia Radiolarite|24059|5|Briefly described|p138|Cretaceous|Cretaceous|Geological Province: Barrow Sub-basin.||||||
20198|Windalia Radiolarite|24084|5|Briefly described|p146 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
20198|Windalia Radiolarite|24160|5|Briefly described|p36, 38|Cretaceous|Cretaceous|Known locally as mookaite, which is mined and sold as a semi-precious stone.||Winning Group||Overlies conformably the Birdrong Sandstone or Muderong Shale. Grades laterally into Nanutarra Formation. Is overlain conformably by Gearle Siltstone, Alinga Formation, Haycock Marl.|Commonly with secondary opaline silicification, with liesegang banding.|
20198|Windalia Radiolarite|24205|5|Briefly described|p242|||Geological Province: Northern Carnarvon Basin.  See also p250 Fig. 6.||||||
20198|Windalia Radiolarite|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Early Cretaceous|Conformably overlies Windalia Sand Member. Conformably overlain by Gearle Siltstone. Marine. Geological Province: Barrow Sub-basin.||||||
20198|Windalia Radiolarite|24351|5|Briefly described|Plate 4 (in pocket)|Early Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province: Exmouth Sub-basin and Gascoyne Platform/Sub-basin.||||||13-DEC-07
20198|Windalia Radiolarite|24410|5|Briefly described|p132, p213|Cretaceous|Cretaceous|Of the Winning Group. Radiolarite, sandy radiolarite and chert; variably porcellanised. Conform. overlies the Birdrong Sst or Muderong Shale; uncon. overlain by Gearle Siltstone; overlain by Alinga Fm. Geol. Prov: Carnarvon Basin.||||||24-NOV-09
20198|Windalia Radiolarite|29381|4|Described|p67|||||||||
20198|Windalia Radiolarite|29721|6|Mentioned|Table 102|||||||||
20198|Windalia Radiolarite|30016|6|Mentioned|p92|||Lower Cretaceous||||||
20198|Windalia Radiolarite|30304|4|Described|p53|||Albian age||||||
20198|Windalia Radiolarite|30365|6|Mentioned|Fig.8|||||||||
20198|Windalia Radiolarite|30443|6|Mentioned|p14|||Aptian - Early Albian age||||||
20198|Windalia Radiolarite|30948|6|Mentioned|Map legend|Albian|Aptian|Albian - Aptian||||||
20198|Windalia Radiolarite|31083|6|Mentioned|Fig. 2|||||||||
20198|Windalia Radiolarite|31561|5|Briefly described|p34|||Early Cretaceous||||||
20198|Windalia Radiolarite|32166|5|Briefly described|p159|||||||||
20198|Windalia Radiolarite|32648|6|Mentioned|p32|||in Winning Gp.||||||
20198|Windalia Radiolarite|32649|4|Described|p26|||See also Table 1||||||
20198|Windalia Radiolarite|33165|6|Mentioned|Chart|||Correlation chart only||||||
20198|Windalia Radiolarite|33386|6|Mentioned|Fig.7|||||||||
20198|Windalia Radiolarite|33450|6|Mentioned|Fig.5|||See P11.||||||
20198|Windalia Radiolarite|33453|4|Described|p72|||Aptain p75.||||||07-NOV-06
20198|Windalia Radiolarite|34363|6|Mentioned|p56|||Aptian - Albian. See Fig.7,8 and P57.||||||
20198|Windalia Radiolarite|34730|6|Mentioned|p78|||||||||
20198|Windalia Radiolarite|34838|6|Mentioned|p3|||||||||
20198|Windalia Radiolarite|34840|6|Mentioned|p69|||||||||
20198|Windalia Radiolarite|34846|6|Mentioned|Fig.3|||||||||
20198|Windalia Radiolarite|35105|6|Mentioned|Fig.5|||||||||
20198|Windalia Radiolarite|35144|6|Mentioned|p5|||||||||
20198|Windalia Radiolarite|35282|6|Mentioned|Fig.19|||||||||
20198|Windalia Radiolarite|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
20198|Windalia Radiolarite|36093|6|Mentioned|Fig.2|||||||||
20198|Windalia Radiolarite|36199|6|Mentioned|p3|||||||||
20198|Windalia Radiolarite|36257|6|Mentioned|Table 2.1|||||||||
20198|Windalia Radiolarite|36552|6|Mentioned|p60|||||||||
20198|Windalia Radiolarite|36751|6|Mentioned|p167|||||||||
20198|Windalia Radiolarite|36890|3|Fully described|p297|||||||||
20198|Windalia Radiolarite|36902|6|Mentioned|p22|||||||||
20198|Windalia Radiolarite|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20198|Windalia Radiolarite|37320|6|Mentioned|p235|||||||||
20198|Windalia Radiolarite|37360|4|Described|p575|||||||||
20198|Windalia Radiolarite|37422|5|Briefly described|p9|||||||||
20198|Windalia Radiolarite|37689|6|Mentioned|p25|||On schematic section.||||||
20198|Windalia Radiolarite|38482|6|Mentioned|p22|||||||||
20198|Windalia Radiolarite|38485|4|Described|p15|||||||||
20198|Windalia Radiolarite|38998|4|Described|p19|||||||||
20198|Windalia Radiolarite|39158|5|Briefly described|p36|||||||||
20198|Windalia Radiolarite|39211|6|Mentioned|p58|||||||||
20198|Windalia Radiolarite|39427|4|Described|Table 1|||||||||
20198|Windalia Radiolarite|39486|6|Mentioned|p2092|||||||||
20198|Windalia Radiolarite|39757|6|Mentioned|p1605|||||||||
20198|Windalia Radiolarite|40340|5|Briefly described|p14|||||||||
20198|Windalia Radiolarite|40341|6|Mentioned|Map legend|Albian|Albian|||||||
20198|Windalia Radiolarite|40342|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20198|Windalia Radiolarite|40343|5|Briefly described|p11|||||||||
20198|Windalia Radiolarite|40617|6|Mentioned|p18|||||||||
20198|Windalia Radiolarite|40800|6|Mentioned|p4|||||||||
20198|Windalia Radiolarite|40801|6|Mentioned|p42|||||||||
20198|Windalia Radiolarite|40877|5|Briefly described|p55|||||||||
20198|Windalia Radiolarite|40992|6|Mentioned|Fig.8|||||||||
20198|Windalia Radiolarite|41125|5|Briefly described|p41|||||||||
20198|Windalia Radiolarite|41158|5|Briefly described|p231|||||||||
20198|Windalia Radiolarite|41170|6|Mentioned|Fig.4|||||||||
20198|Windalia Radiolarite|41271|3|Fully described|p150|||See also p18.||||||07-NOV-06
20198|Windalia Radiolarite|41436|6|Mentioned|p48|||||||||
20198|Windalia Radiolarite|41438|6|Mentioned|p108|||||||||
20198|Windalia Radiolarite|41439|5|Briefly described|p122|||||||||
20198|Windalia Radiolarite|41440|4|Described|p138|||||||||
20198|Windalia Radiolarite|41443|6|Mentioned|Fig.3|||||||||
20198|Windalia Radiolarite|41444|6|Mentioned|Fig.4|||||||||
20198|Windalia Radiolarite|41445|6|Mentioned|Fig.4|||||||||
20198|Windalia Radiolarite|41446|6|Mentioned|Fig.2|||||||||
20198|Windalia Radiolarite|41447|6|Mentioned|Fig.3|||||||||
20198|Windalia Radiolarite|41533|6|Mentioned|p265|||||||||
20198|Windalia Radiolarite|41712|6|Mentioned|Fig.8|||||||||
20198|Windalia Radiolarite|41732|6|Mentioned|Fig.3|||||||||
20198|Windalia Radiolarite|42116|5|Briefly described|p18|||See also Fig.1||||||
20198|Windalia Radiolarite|42123|6|Mentioned|p15|||||||||
20198|Windalia Radiolarite|42393|5|Briefly described|Fig. 2 P103|||||||||
20198|Windalia Radiolarite|42463|6|Mentioned|Fig.2 P169|||||||||
20198|Windalia Radiolarite|42598|5|Briefly described|p95|||||||||
20198|Windalia Radiolarite|42995|5|Briefly described|p15|||See also Table 1.||||||
20198|Windalia Radiolarite|43564|6|Mentioned|p445|Albian|Aptian|(L.Aptian-E.Albian)||||||
20198|Windalia Radiolarite|43598|6|Mentioned|p813|Albian|Aptian|(Late Aptian-Early Albian)||||||
20198|Windalia Radiolarite|43712|5|Briefly described|p11||Aptian|||||||
20198|Windalia Radiolarite|43722|5|Briefly described|p10-11|||||||||
20198|Windalia Radiolarite|43724|5|Briefly described|p29,30||Aptian|||||||
20198|Windalia Radiolarite|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
20198|Windalia Radiolarite|44159|5|Briefly described|Table p.37||Early Cretaceous|||||||
20198|Windalia Radiolarite|44344|14|Not recorded|p.17-19,24,opp.4,map|Albian|Aptian|Aptian-L.Albian; fm. of Winning Group. (G50-1)||||||
20198|Windalia Radiolarite|44345|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
20198|Windalia Radiolarite|44532|4|Described|p.9, map|||(G50-5).||||||
20198|Windalia Radiolarite|44533|5|Briefly described|map legend||Early Cretaceous|Lower Cretaceous.||||||
20198|Windalia Radiolarite|44537|14|Not recorded|map legend||Late Cretaceous|Upper Cretaceous.||||||
20198|Windalia Radiolarite|44657|14|Not recorded|p.5,6,11,12|||||||||
20198|Windalia Radiolarite|44992|14|Not recorded|?|||||||||
20198|Windalia Radiolarite|44996|14|Not recorded|p.10|Albian|Aptian|(ref to Brunnschweiler, 1959.)||||||
20198|Windalia Radiolarite|44998|14|Not recorded|p164,169,188|||||||||
20198|Windalia Radiolarite|45004|14|Not recorded|p.8|||Tb.1.||||||
20198|Windalia Radiolarite|45005|14|Not recorded|?|||||||||
20198|Windalia Radiolarite|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||01-JUN-06
20198|Windalia Radiolarite|45016|14|Not recorded|p.128,181||Cretaceous|Cretaceous.||||||
20198|Windalia Radiolarite|45142|6|Mentioned|Fig.4|||||||||
20198|Windalia Radiolarite|45149|6|Mentioned|Table 1|||Page 15.||||||
20198|Windalia Radiolarite|47053|6|Mentioned|p471|||||||||
20198|Windalia Radiolarite|48610|14|Not recorded|Pl.1,5,6|||||||||
20198|Windalia Radiolarite|48628|14|Not recorded|p23|||(F50-5/Onslow).||||||
20198|Windalia Radiolarite|48831|14|Not recorded|p79,81|||||||||
20198|Windalia Radiolarite|48858|14|Not recorded|p.5|||(G50-1/Norton).||||||
20198|Windalia Radiolarite|48861|2|Defined|p.7|||p.1,5,9, Pl.1.||||||
20198|Windalia Radiolarite|49942|4|Described|p4 Fig.3|Early Cretaceous|Early Cretaceous|Conformably overlain by Gearle Siltstone and Alinga Formation. Conformably overlies Muderong Shale. Of Winning Group. Siliceous. Geological Province: Gascoyne Platform.||||||
20198|Windalia Radiolarite|50085|5|Briefly described|p23 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
20198|Windalia Radiolarite|60119|6|Mentioned|p26|||Possibly oil-bearing.  Geological Province: Carnarvon Basin.||||||
20198|Windalia Radiolarite|60379|6|Mentioned|p126 fig 3|Albian|Albian|Dampier sub-basin, Carnarvon Basin||||||
20198|Windalia Radiolarite|60384|5|Briefly described|p243 Fig 2a, p261|Early Cretaceous|Early Cretaceous|Perth and Carnarvon Basins.||Of Winning Group.||||
20198|Windalia Radiolarite|60386|6|Mentioned|p302|Aptian|Barremian|Perth Basin, Carnarvon Basin. Shown at two distinct stratigraphic levels: one Barremian, one Aptian. Limestone nearshore-shelf.||||||
20198|Windalia Radiolarite|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|||||||
20198|Windalia Radiolarite|61555|6|Mentioned|p235|||Contains tight gas in Pyrenees-1.||||||
20198|Windalia Radiolarite|61811|4|Described|p3 Fig.2, p8, p9 Table 3, p11, pp13-15. |Aptian|Aptian|Northern Perth Basin. Helminthopis and Zoophycus ichnofacies.||Unit in Winning Group.||Overlies Windalia Sandstone Member. Is overlain by Alinga Formation.|Alternating friable and moderately indurated radiolarite-rich mudstone and siltstone, and indurated radiolarite beds; belemnite moulds in mudstone beds.|
20198|Windalia Radiolarite|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||
20198|Windalia Radiolarite|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
20198|Windalia Radiolarite|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Contains Windalia Sand Member. Overlain by Gearle Sandstone.  Age: 110Ma. Geological Province: Exmouth Sub-basin, Barrow Sub-basin, Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
20198|Windalia Radiolarite|63950|5|Briefly described|p336 Fig. 4|Albian|Aptian|Overlies Muderong Shale; underlies the lower section of Gearle Siltstone. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
20198|Windalia Radiolarite|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
20198|Windalia Radiolarite|64635|5|Briefly described|p4 Fig.3, p7  |Aptian|Aptian|||Unit in Winning Group.||||
20198|Windalia Radiolarite|64972|6|Mentioned|p616|Cretaceous|Cretaceous|||||||
20198|Windalia Radiolarite|64973|4|Described|p504, p504 Fig. 2, p506 Fig. 4|Aptian|Aptian|Of Winning Group. Geological Province: Carnarvon Basin. Deposited under conditions of starved terrigenous influx. Also on p506 Fig. 6, p509, p510.||||||01-SEP-14
20198|Windalia Radiolarite|64977|6|Mentioned|p493 Fig.3.|Early Cretaceous|Early Cretaceous|Thevenard Island area.||Unit in Muderong Shale.||Overlies Windalia Sand Member. Is overlain by Gearle Siltstone.||
20198|Windalia Radiolarite|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
20198|Windalia Radiolarite|67195|5|Briefly described|Appendix 2 p8|||Carnarvon Basin.|||||Includes grey mudstone, not dense.|04-JAN-23
20198|Windalia Radiolarite|67200|5|Briefly described|p8 fig 6, p17 table 1|Cretaceous|Cretaceous|Thermal conductivity of 1.45 W/mK. See also p49, p50, p53, app 2 p8.||Winning Group||Overlies Muderong Shale, Windalia Sandstone Member, overlain by Alinga Formation, Gearle Siltstone, Haycock Marl|Crudely bedded radiolarite, siltstone and mudstone.|
20198|Windalia Radiolarite|67340|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|Northern Perth Basin.||Winning Group.|Windalia Sandstone Member.|||
20198|Windalia Radiolarite|67368|6|Mentioned|p209 Fig.4.|Albian|Aptian|||||Overlies Muderong Shale. Is overlain by Haycock Marl.||
20198|Windalia Radiolarite|67784|5|Briefly described|p26, p28 table 1, p30, p31, p32, p33|Aptian|Aptian|Carnarvon Basin. 30-47m thick.||||Overlies Windalia Sand Member (Muderong Shale); overlain paraconformably by Gearle Siltstone.|A distinctive siliceous radiolarian-rich siltstone.|08-FEB-18
20198|Windalia Radiolarite|67970|5|Briefly described|p25 Fig.4.|Aptian|Aptian|Exmouth Plateau.||Unit in Winning Group.||Is overlain by Gearle Siltstone.||
20198|Windalia Radiolarite|68206|6|Mentioned|p29-30, 32-33|Aptian|Aptian|Carnarvon Basin.||||Overlies Muderong Shale. Is overlain by Gearle Siltstone.||
20198|Windalia Radiolarite|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
20198|Windalia Radiolarite|69182|5|Briefly described|Ch3 p8, Ch3 p12-p13|Cretaceous|Cretaceous|Carnarvon Basin. Has favourable porosity and permeability characteristics, however it is never deep enough to act as a storage reservoir for carbon dioxide. See also Ch3 p17-p18 Ch3 p23-p27, Ch3 p29, Ch3 p34, Ch3 p35, Ch3 p37, Ch3 p65-p66, Ch3 p69, Ch3 p71, Ch3 p73.||||Overlies the Muderong Shale. Overlain by the Gearle Siltstone.|Fine-grained, silica rich radiolarite|
20198|Windalia Radiolarite|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.||||
20198|Windalia Radiolarite|69297|5|Briefly described|p247, p249|Aptian|Aptian|Gascoyne Sub-basin of the Southern Carnarvon Basin. Deposited in a shallow marine environment.||Winning Group||Overlies the Windalia Sand Member. Overlain by the Gearle Siltstone.|Uniform white radiolarian siltstone.|
20198|Windalia Radiolarite|69558|6|Mentioned|p258 fig 419|Early Cretaceous|Early Cretaceous|||||Overlies the Muderong Shale. Overlain by the Gearle Siltstone. Faulted against the Birdrong Sandstone.||25-MAY-21
20198|Windalia Radiolarite|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||Overlies Muderong Shale.||
20198|Windalia Radiolarite|69692|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||||Overlies Muderong Formation and Windalia Sandstone. Is overlain by Lower Gearle Siltstone.||
20198|Windalia Radiolarite|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Albian|Aptian|See also Regional: Fig.6; p6, p9. Northern Carnarvon Basin. Forms a top-seal for the Barrow Island oil field in the Barrow Sub-basin.||Winning Group.||Overlies Windalia Sand Member or Muderong Shale. Is overlain by Gearle Siltstone.||
20198|Windalia Radiolarite|70906|5|Briefly described|p757-758|Early Cretaceous|Early Cretaceous|Gorgon Platform.||||Overlies Muderong Shale. Is overlain by Siltstone.||
20198|Windalia Radiolarite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||radiolarite|
20198|Windalia Radiolarite|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Plateau.||||Overlies Muderong Shale. Is overlain by Gearle Siltstone.||
20202|Windalia Sand Member|23379|4|Described|p160 Fig.2; p158-161,164,165,171-174||Aptian|Invalid name - Windalia Radiolarite has priority. Of Muderong Shale, Barrow Sub-basin, Carnarvon Basin.||||||07-NOV-06
20202|Windalia Sand Member|23535|5|Briefly described|p125 Fig 3|||Of Muderong Shale.||||||
20202|Windalia Sand Member|23726|5|Briefly described|p8 Fig 2c|Early Cretaceous|Early Cretaceous|Overlain by Windalia Radiolarite. Underlain by Muderong Shale. Geological Province: Carnarvon Basin.||||||07-NOV-06
20202|Windalia Sand Member|24059|4|Described|p132|Late Cretaceous|Early Cretaceous|Of Muderong Shale. Geological Province: Barrow Sub-basin.||||||
20202|Windalia Sand Member|24205|5|Briefly described|p242|||Of the Muderong Shale.  Geological Province: Northern Carnarvon Basin.||||||
20202|Windalia Sand Member|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Early Cretaceous|Conformably overlies Muderong Shale. Conformably overlain by Windalia Radiolarite. Marine. Geological Province: Barrow Sub-basin.||||||
20202|Windalia Sand Member|24351|5|Briefly described|Plate 4 (in pocket)|Early Cretaceous|Early Cretaceous|Of the Windalia Radiolarite (Winning Group). Geological Province: Exmouth Sub-basin (offshore).||||||13-DEC-07
20202|Windalia Sand Member|30304|4|Described|p52|||Aptian to Albian age. Member of Muderong Shale.||||||07-NOV-06
20202|Windalia Sand Member|31083|6|Mentioned|Fig. 2|||||||||
20202|Windalia Sand Member|33450|6|Mentioned|Fig.5|||See P11.||||||
20202|Windalia Sand Member|33453|4|Described|p72|||Aptian p75.||||||07-NOV-06
20202|Windalia Sand Member|34846|6|Mentioned|Fig.3|||||||||
20202|Windalia Sand Member|35144|6|Mentioned|Fig.5|||||||||
20202|Windalia Sand Member|35282|6|Mentioned|Fig.21|||||||||
20202|Windalia Sand Member|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
20202|Windalia Sand Member|36266|6|Mentioned|p152|||||||||
20202|Windalia Sand Member|37320|6|Mentioned|p237|||||||||
20202|Windalia Sand Member|39486|6|Mentioned|p2092|||See also Fig.2||||||
20202|Windalia Sand Member|40617|5|Briefly described|p14|||||||||
20202|Windalia Sand Member|40992|6|Mentioned|p6|||||||||
20202|Windalia Sand Member|41271|3|Fully described|p148|||||||||
20202|Windalia Sand Member|41439|4|Described|p116|||||||||
20202|Windalia Sand Member|41440|5|Briefly described|p138|||||||||
20202|Windalia Sand Member|41441|6|Mentioned|p153|||||||||
20202|Windalia Sand Member|41446|6|Mentioned|Fig.2|||||||||
20202|Windalia Sand Member|41732|5|Briefly described|p540|||||||||
20202|Windalia Sand Member|42116|5|Briefly described|p47|||||||||
20202|Windalia Sand Member|42598|4|Described|P 99|early Aptian|late Barremian|Invalid name (Windalia Radiolarite is older), but entrenched in industry and literature.||||||07-NOV-06
20202|Windalia Sand Member|43564|6|Mentioned|p447|||||||||
20202|Windalia Sand Member|45142|6|Mentioned|p8|||||||||
20202|Windalia Sand Member|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Forms part of Windalia Radiolarite. Age: 110Ma. Geological Province: Barrow Sub-basin and Exmouth Sub-basin.||||||01-MAR-10
20202|Windalia Sand Member|64977|6|Mentioned|p493 Fig.3.|Early Cretaceous|Early Cretaceous|Thevenard Island area.||Unit in Muderong Shale.||Is overlain by Windalia Radiolarite.||
20202|Windalia Sand Member|67784|5|Briefly described|p26|||Carnarvon Basin. 10-32m thick.||Muderong Shale||Is overlain by Windalia Radiolarite.||08-FEB-18
20202|Windalia Sand Member|69297|5|Briefly described|p249|Aptian|Aptian|Gascoyne Sub-basin of the Southern Carnarvon Basin.||Muderong Shale||Overlies the Muderong Shale. Overlain by the Windalia Radiolarite.|Sandstone.|
20202|Windalia Sand Member|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
20202|Windalia Sand Member|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Aptian|Aptian|See also Regional: Fig.6; p6-7, p16. Northern Carnarvon Basin. The primary reservoir of the Barrow Island oil field; contained over 90% of the initial oil reserves. Appears as Windalia Sandstone Member on p16.||Muderong Shale.||Is overlain by Windalia Radiolarite.||
20226|Windjana Limestone|22550|6|Mentioned|Fig 3|||||||||
20226|Windjana Limestone|22741|6|Mentioned|P22||Devonian|||||||
20226|Windjana Limestone|23722|4|Described|p31|Devonian|Devonian|Geological Province: Canning Basin.||||||10-NOV-08
20226|Windjana Limestone|23847|5|Briefly described|p296|Famennian|Famennian|Geological Province: Canning Basin.||||||
20226|Windjana Limestone|23903|5|Briefly described|p1597 Fig.2|Famennian|Famennian|Geological Province: Canning Basin.||||||10-NOV-08
20226|Windjana Limestone|24061|5|Briefly described|p180|Late Devonian|Middle Devonian|Geological Province: Canning Basin.||||||10-NOV-08
20226|Windjana Limestone|24371|5|Briefly described|p206|Famennian|Famennian|Reef magin and slope. Unconformably overlies Napier and Pillara Formations. Geological province: Canning Basin.||||||
20226|Windjana Limestone|30110|6|Mentioned|p81|||See also P82. Upper Devonian, Frasnian-Famennian age.||||||
20226|Windjana Limestone|30525|6|Mentioned|Map legend|Famennian|Frasnian|Famennian to Frasnian||||||
20226|Windjana Limestone|30533|4|Described|p24|||On Table 6.||||||13-NOV-07
20226|Windjana Limestone|30897|4|Described|p18|||Stratigraphic table p17.||||||13-NOV-07
20226|Windjana Limestone|30898|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian - Famennian||||||
20226|Windjana Limestone|31152|6|Mentioned|Fig. 3|||||||||
20226|Windjana Limestone|31332|6|Mentioned|Fig. 3|||||||||
20226|Windjana Limestone|32594|6|Mentioned|p3|||Refers Playford & Lowry (1966)||||||
20226|Windjana Limestone|32619|6|Mentioned|p464|||Givetian||||||
20226|Windjana Limestone|32647|1|Redefined|p100|Famennian|Famennian|||||||
20226|Windjana Limestone|32648|6|Mentioned|p32|||Devonian||||||
20226|Windjana Limestone|32825|5|Briefly described|p566|||Frasnian and Famennian. Reef facies.||||||10-NOV-08
20226|Windjana Limestone|32865|6|Mentioned|p473|||Givetian to Late Fammenian||||||
20226|Windjana Limestone|33042|6|Mentioned|p725|||Frasnian. See also P731,732,747-750 etc.||||||
20226|Windjana Limestone|34427|6|Mentioned|Fig.3|||||||||
20226|Windjana Limestone|34999|6|Mentioned|p124|||||||||
20226|Windjana Limestone|35104|6|Mentioned|p4|||||||||
20226|Windjana Limestone|36115|6|Mentioned|p133|||||||||
20226|Windjana Limestone|36365|6|Mentioned|p821|||||||||
20226|Windjana Limestone|36890|3|Fully described|p330|||||||||
20226|Windjana Limestone|38207|6|Mentioned|Fig.1|||||||||
20226|Windjana Limestone|39702|6|Mentioned|Fig.2|||||||||
20226|Windjana Limestone|40236|6|Mentioned|Fig.5|||||||||
20226|Windjana Limestone|40793|6|Mentioned|Fig.3|||||||||
20226|Windjana Limestone|40797|6|Mentioned|Fig.2|||||||||
20226|Windjana Limestone|40838|6|Mentioned|p278|||||||||
20226|Windjana Limestone|41139|6|Mentioned|p1489|||||||||
20226|Windjana Limestone|41158|6|Mentioned|p80|||See also Plate 2||||||
20226|Windjana Limestone|41217|5|Briefly described|Fig.2|||||||||
20226|Windjana Limestone|41894|5|Briefly described|p4|||||||||
20226|Windjana Limestone|41918|5|Briefly described|p103|||||||||
20226|Windjana Limestone|42030|6|Mentioned|p748|||||||||
20226|Windjana Limestone|42080|6|Mentioned|Fig.2 P281|||||||||
20226|Windjana Limestone|42111|6|Mentioned|Text fig.3 P90|||||||||
20226|Windjana Limestone|42351|5|Briefly described|Fig.3 P40|||||||||
20226|Windjana Limestone|42564|5|Briefly described|Fig.5, 6 P6|||||||||
20226|Windjana Limestone|42710|5|Briefly described|map legend|Late Devonian||||||||
20226|Windjana Limestone|42811|4|Described|p42|||see also Fig.9.||||||13-NOV-07
20226|Windjana Limestone|42814|5|Briefly described|p22|||||||||
20226|Windjana Limestone|42815|5|Briefly described|map|Late Devonian||||||||
20226|Windjana Limestone|42860|5|Briefly described|Fig.2|||||||||
20226|Windjana Limestone|42930|5|Briefly described|Fig.1 p473|Late Devonian|Late Devonian|Partly underlies and interfingers with Nullara Limestone. Geological Province: Canning Basin.||||||13-NOV-07
20226|Windjana Limestone|42933|5|Briefly described|Fig.94 p258|||||||||
20226|Windjana Limestone|43173|6|Mentioned|54||Late Devonian|||||||
20226|Windjana Limestone|43281|6|Mentioned|Map legend||Late Devonian|||||||
20226|Windjana Limestone|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
20226|Windjana Limestone|43723|6|Mentioned|p53||Devonian|||||||
20226|Windjana Limestone|44143|4|Described|p438 Table 4-19, p442, p443 Figure 4-98|Devonian|Devonian|Up to 150m thick; massive limestone; shallow marine. Interfingers with Nullara Limestone. Type section at Windjana Gorge where Lennard River cuts through Napier Range (LENNARD RIVER: 17deg 24' 30" S, 124deg 57' 30" E). Contains algae, brachiopods and corals; Famennian.||||||24-NOV-17
20226|Windjana Limestone|44231|5|Briefly described|Map Legend|Famennian|Famennian|Reef-margin subfacies: massive cyanobacterial limestone and dolomite. Geological Province: Canning Basin.||||||19-MAY-05
20226|Windjana Limestone|44366|14|Not recorded|p.19, Table 3|||Givetian (?) to Famennian.||||||
20226|Windjana Limestone|44367|14|Not recorded|map legend|||(Reprinted 1971), Givetian? to Famennian.||||||
20226|Windjana Limestone|44397|14|Not recorded|p.11, Figs.2,3.Tb.4|||Frasnian to (?) Givetian.||||||
20226|Windjana Limestone|44398|14|Not recorded|map legend|||Givetian (?) to Famennian.||||||
20226|Windjana Limestone|45041|6|Mentioned|Fig.45|||Devonian||||||
20226|Windjana Limestone|45063|6|Mentioned|Fig. 9|||Dev.||||||
20226|Windjana Limestone|45101|6|Mentioned|p5|||See also P21. Conodont content||||||
20226|Windjana Limestone|45133|6|Mentioned|Fig.3|||||||||
20226|Windjana Limestone|45143|6|Mentioned|Fig.4|||Geology of the Fairfield Group.||||||
20226|Windjana Limestone|45153|2|Defined|App.3-55|Famennian|Famennian|||||||
20226|Windjana Limestone|45158|4|Described|p24|||||||||
20226|Windjana Limestone|46869|6|Mentioned|Fig.1|||||||||
20226|Windjana Limestone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
20226|Windjana Limestone|63938|5|Briefly described|p50 Fig.2|Famennian|Famennian|||||||
20226|Windjana Limestone|64159|5|Briefly described|p91 Fig. 6|Famennian|Famennian|Part of the Lennard Reef facies development.||||||
20226|Windjana Limestone|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Underlain by Virgin Hills Formation, overlain by Nullara Limestone. Limestone, dolomite (shallow marine). Geological Province: Canning Basin.||||||08-FEB-10
20226|Windjana Limestone|64502|5|Briefly described|p765 Fig. 2|Famennian|Famennian|||||||
20226|Windjana Limestone|64580|6|Mentioned|map legend|||Fammenian reef complexes, platform facies.||||||15-DEC-08
20226|Windjana Limestone|64643|5|Briefly described|p6, p7 Fig. 5, p35|Famennian|Famennian|Reefal deposits.||||||24-NOV-08
20226|Windjana Limestone|65486|5|Briefly described|p6-7,9,37,47; Figs.5,6,7,50; Plate 1|Late Famennian|Middle Famennian|Reef, back-reef, and bank limestone, dolomite and sandstone, Canning Basin. Underlies and interfingers with Nullara Limestone. Overlies and interfingers with Virgin Hills, Napier and Piker Hills Formation. Unconformably underlies Fairfield Group.||||||
20226|Windjana Limestone|66127|3|Fully described|pp19-21, pp43-46, p332 Fig.457, p377. |Famennian|Famennian|Of Playford and Lowry (1966), for Givetian-Frasnian and Famennian reef facies of the Devonian reef complexes; restricted to Famennian reef-margin and reef-flat deposits by Playford and Cockbain (1976) and Playford (1980). Named after Windjana Gorge; type section extends along the SE wall near the west entrance. Large allochthonous blocks of Windjana Limestone (reef) in the fore-reef subfacies are mapped separately. No outcrop in Plates 4 and 5 areas; shown in Stratigraphic Relationships diagram. Shown on Plates 2, 3, 4, 5, 7, 8.||||Interfingers with Nullara Limestone and Napier Formation. Unconformably overlain by Fairfield Group.|Massive to very crudely bedded limestone; white to pale red; microbial (esp. Renalcis), lesser receptaculitid, sponge and stromatoporoid limestone. Reef-margin facies: massive, microbial reef limestone; locally dolomitized, neptunian dykes common.|
20226|Windjana Limestone|67131|6|Mentioned|p3 Fig. 2,|Famennian|Famennian|Reef subfacies.||||Overlies Pillara Limestone. Overlain by Gumhole Formation.||
20226|Windjana Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Famennian|Fammenian reef complexes, platform facies||||||
20226|Windjana Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
20226|Windjana Limestone|69312|6|Mentioned|p19|Devonian|Devonian|Canning Basin.||||Overlies the Poulton Formation. Overlain by the Virgin Hills Formation.||
20226|Windjana Limestone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Massive to crudely bedded cyanobacterial and minor stromatoporoid reef limestone with contemporaneous deposition of microcrystalline calcite|
20226|Windjana Limestone|71892|6|Mentioned|p8, p10|Late Devonian|Late Devonian|Intruded by Ellendale diamondiferous pipe 4 (E4).|||||Limestones.|
20226|Windjana Limestone|72502|6|Mentioned|p3, p5|Famennian|Frasnian|Lennard Shelf, Canning Basin.||||Underlain by Pillara Limestone. Equivalent to Bugle Gap Formation and Nullara Limestone.||
20256|Winnecke Granophyre|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1830-1815 Ma.||||||19-DEC-06
20256|Winnecke Granophyre|23621|5|Briefly described|p39|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|23809|5|Briefly described|p13|Paleoproterozoic|Paleoproterozoic|Of the Winnecke Suite.  Age: 1815+/-5Ma (Ozchron, AGSO).||||||07-NOV-08
20256|Winnecke Granophyre|24197|5|Briefly described|p7, p26|Proterozoic|Proterozoic|Of the Granites Supersuite. Geological Province: Granites-Tanami Block.||||||07-FEB-11
20256|Winnecke Granophyre|29804|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|29805|4|Described|Table 1|||||||||
20256|Winnecke Granophyre|29809|6|Mentioned|p417|||||||||
20256|Winnecke Granophyre|29811|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|31361|4|Described|Table 1|||See also age Table 2.||||||
20256|Winnecke Granophyre|31412|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|35231|4|Described|Table.1|||||||||
20256|Winnecke Granophyre|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|39571|6|Mentioned|p130|||||||||
20256|Winnecke Granophyre|39887|6|Mentioned|p453|||||||||
20256|Winnecke Granophyre|39888|6|Mentioned|Fig.7|||||||||
20256|Winnecke Granophyre|41465|6|Mentioned|p9|||||||||
20256|Winnecke Granophyre|41961|6|Mentioned|Table 1 P39|||||||||
20256|Winnecke Granophyre|41977|6|Mentioned|p483|||||||||
20256|Winnecke Granophyre|42504|5|Briefly described|Table 3 P60|||||||||
20256|Winnecke Granophyre|42754|6|Mentioned|p3|||||||||
20256|Winnecke Granophyre|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|44965|14|Not recorded|Not recorded|||||||||
20256|Winnecke Granophyre|45140|2|Defined|p12-13, p15, p18, p21-25, p30, p32-35|Paleoproterozoic|Paleoproterozoic|See also p37-39, p41, p62, p70, p74, Appx.p8-9. Traves (1955); Blake et al. (1975). Named after Winnecke Creek. The Granites-Tanami Block. The type area is at 18deg 46'S, 130deg 12'E on the W side of the Tanami-Hooker Creek track to the N of Winnecke Creek. Is probably co-magmatic with the acid lavas of the Mount Winnecke Formation. Has a thin metamorphic aureole. Described as an epizonal pluton. Chemically similar to Slatey Creek Granite; geochemistry detailed.|1802 +/- 15 Ma (Rb-Sr: Page et al., 1976).|||Intrudes the Tanami Complex and Mount Winnecke Formation. Is overlain by Antrim Plateau Volcanics,and ?Gardiner Sandstone against which it is faulted.|Granophyre, pale pink to grey, commonly porphyritic; adamellite, coarser-grained and generally non-porphyritic, occasional small dark xenoliths; and intrusive acid porphyry; locally cut by thin aplitic and andesitic veins or dykes.|
20256|Winnecke Granophyre|46788|4|Described|p4|||||||||
20256|Winnecke Granophyre|46797|6|Mentioned|p80|||Dates given||||||
20256|Winnecke Granophyre|46864|6|Mentioned|p37|||Age dates discussed.||||||
20256|Winnecke Granophyre|48950|2|Defined|p29|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20256|Winnecke Granophyre|50589|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Granites Suite/Supersuite. Geological Province: Granites-Tanami Block. Age: 1815-1764 +/- 15Ma (Shrimp, Rb-Sr).||||||07-NOV-08
20256|Winnecke Granophyre|61056|5|Briefly described|p778, p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Included as part of the Mount Winnecke Formation.  Age: ca. 1830-1815Ma. See also "Winnecke Granophyre".||||||07-NOV-08
20256|Winnecke Granophyre|62580|5|Briefly described|p14, p47|||Intrusive of the Winnecke Suite.||||||07-FEB-11
20256|Winnecke Granophyre|63261|5|Briefly described|p12, p15|Paleoproterozoic|Paleoproterozoic|Part of Birthday Suite. Age: 1815Ma. Geochemically equivalent to the rhyolite within Mount Winnecke Formation. Commonly porphyritic, biotite-bearing; includes medium- to coarse-grained monzogranite and granodiorite with micrographic/myrmekitic textures.||||||07-FEB-11
20256|Winnecke Granophyre|64662|6|Mentioned|p43|Orosirian|Orosirian|Age: 1815+/-5Ma. Intrudes Ware Group.||||||07-FEB-11
20256|Winnecke Granophyre|64677|6|Mentioned|p20|||||||Intrudes Helena Creek beds.||
20256|Winnecke Granophyre|64733|6|Mentioned|p173|||High-level intrusive. Emplacement accompanied deposition of Ware Group.||||||20-APR-12
20256|Winnecke Granophyre|65358|5|Briefly described|p9-10, p9 Fig.8|||Of Birthday Suite. Has auriferous quartz veins.||||||
20256|Winnecke Granophyre|65359|4|Described|p1-38.|Statherian|Orosirian|Tanami Region. Intrudes Mount Winnecke Formation; comagmatic with Mount Winnecke Formation's volcanic component. Biotite granophyre, biotite-quartz-monzonite, biotite-hornblende syenogranite, quartz-feldspar porphyry, intrusive acid porphyry. Geochemistry detailed. 1815+/-5 Ma; SHRIMP U-Pb zircon (Ozchron). Abundant Zn and Sn.||||||
20256|Winnecke Granophyre|69426|5|Briefly described|p11:4 Fig.11.3, 11:7, 10-12|Orosirian|Orosirian|Magmatic crystallisation age.|1815 +/- 5 Ma (Page, 1998).|Birthday Suite.||Intrudes Mount Winnecke Formation.|Granophyre, quartz-feldspar porphyry and syenogranite; commonly porphyritic; features quartz, alkali feldspar, plagioclase and brown biotite in a quartz and alkali feldspar groundmass. Also medium- to coarse-grained monzogranite and granodiorite.|12-JUL-16
20256|Winnecke Granophyre|70291|5|Briefly described|p180-181|Orosirian|Orosirian|Geological province: Tanami. Coeval with deposition of, and intrudes Ware Group.||Unit of Birthday Suite.||||
20256|Winnecke Granophyre|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1815 Ma.|Birthday Suite.|||Biotite-bearing syenogranite, monzogranite, including minor quartz-feldspar porphyry, quartz-phyric rhyolite.|
20256|Winnecke Granophyre|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granophyre|
20256|Winnecke Granophyre|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1815+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granophyre.|
20256|Winnecke Granophyre|73089|5|Briefly described|p8, p39|Orosirian|Orosirian|Considered to be part of the same magmatic event that produced the felsic volcanic rocks [of the Ware Group?].|1815 +/- 5 Ma [1825 +/- 5 Ma elsewhere?]|Birthday Suite||Intrudes Mount Winnecke Formation.||
20259|Winning Group|6943|6|Mentioned|p606.|Lower Cretaceous|Lower Cretaceous|||||Unconformably overlies Sweeney Mia Formation.||
20259|Winning Group|12471|6|Mentioned|p475 Fig.2.|Late Cretaceous|Early Cretaceous||||Includes Birdrong Sandstone, Muderong Shale (includes Mardie Greensand Member, Windalia Sandstone Member), Windalia Radiolarite, and Gearle Siltstone.|||27-OCT-14
20259|Winning Group|12729|5|Briefly described|p.15, 17, 20, 28, 32, 34, Fig. 6.|Late Cretaceous|Early Cretaceous|Maximum thickness: ~600 m. Deposited during a transgression (Neocomian to Cenomanian).|||Birdrong Sandstone, Muderong Shale, Windalia Sandstone Member, Windalia Radiolarite, Gearle Siltstone, Alinga Formation|Disconformably overlain by the Toolonga Calcilutite.|Sandstone, shale, siliceous shale.|
20259|Winning Group|12731|6|Mentioned|p592.|Early Cretaceous|Early Cretaceous|Onshore southern Carnarvon Basin. Thinning of this unit over a broad anticline indicates that deformation continued for some time after breakup from Greater India.|||Includes Birdrong Sandstone.|||
20259|Winning Group|13615|4|Described|p1, p18, 19, p30-p32,|Turonian|Hauterivian|Peedamullah Shelf. Marine clastic sedimentary section. Petrochemistry in drillholes is provided. Intersected in numerous drillholes. See also p35, p43, p51, p56, p58, p65, p85, p88, p101 App. 3.|||Includes the Birdrong Sandstone, Mardie Greensand, Windalia Radiolarite, Gearle Siltstone, Muderong Shale.|Unconformably overlies the Barrow Group.||12-FEB-19
20259|Winning Group|14228|5|Briefly described|p5 fig 2, p9, p16-18|Cretaceous|Berriasian|Mudstone facies have generated hydrocarbons in Northern Carnarvon Basin.|||Birdrong Sandstone, Muderong Shale, Windalia Radiolarite, Gearle Siltstone, Alinga Formation.|Overlain by Haycock Marl.||
20259|Winning Group|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
20259|Winning Group|23311|5|Briefly described|map legend|Late Cretaceous|Early Cretaceous|||||||
20259|Winning Group|23312|5|Briefly described|map legend|Late Cretaceous|Early Cretaceous|||||||
20259|Winning Group|23355|5|Briefly described|13|Cretaceous|Cretaceous|||||||
20259|Winning Group|23403|4|Described|p8|Cretaceous|Cretaceous|||||||24-NOV-09
20259|Winning Group|23520|5|Briefly described|p6 Fig. 4|Early Cretaceous|Early Cretaceous|Geological Province: Abrolhos Sub-basin.  See also p12.||||||
20259|Winning Group|23535|6|Mentioned|Figure 3 p127.|||Geological Province: Southern Carnarvon Basin.||||||
20259|Winning Group|23572|4|Described|p11|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Overlying Unit: Toolonga Calcilutite (disconformable). Max. thickness: 600m.||||||
20259|Winning Group|23620|5|Briefly described|p4 Fig. 4|Cretaceous|Cretaceous|Marine and coastal shale, siltstone and radiolarite: dominantly siliceous pelagic deposits with basal sandstone and conglomerate.||||||07-OCT-20
20259|Winning Group|23726|5|Briefly described|p69|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin.||||||
20259|Winning Group|23815|5|Briefly described|p295|Turonian|Neocomian|Formerly known as "Winning Series". Geological Province: Carnarvon Basin.||||||
20259|Winning Group|23935|5|Briefly described|p11 Fig.7|Turonian|Neocomian|Unconformably overlain by Toolonga Calcilutite. Geological Province: Southern Carnarvon Basin.||||||
20259|Winning Group|23976|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
20259|Winning Group|23977|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
20259|Winning Group|23978|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
20259|Winning Group|24059|4|Described|p132|Late Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||
20259|Winning Group|24160|4|Described|p36, p37, 38|Cretaceous|Cretaceous||||Birdrong Sandstone, Muderong Shale, Windalia Radiolarite, Gearle Siltstone, Alinga Formation, Haycock Marl.||Sandstone, siltstone, conglomerate.|
20259|Winning Group|24351|5|Briefly described|p16, Plate 4 (in pocket)|Late Cretaceous|Early Cretaceous|Includes Birdrong Sandstone, Muderong Shale, "Windalia Sand", Windaila Radiolarite, Alinga Formation and Gearle Siltstone. Geol.Prov: Gascoyne Platform/Sub-basin and Exmouth Sub-basin. Shallow marine claystones and siltstones. Age: Aptian-Cenomanian||||||13-DEC-07
20259|Winning Group|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
20259|Winning Group|24410|5|Briefly described|p132|Cretaceous|Cretaceous|Siliciclastic sequence including Birdrong Sandstone, Windalia Radiolarite and Alinga Formation. Shale, siltstone, greensand, radiolarite and sandstone. Geological Province: Carnarvon Basin.||||||24-NOV-09
20259|Winning Group|29381|6|Mentioned|p67|||See also Table.||||||
20259|Winning Group|29721|6|Mentioned|p102|||||||||
20259|Winning Group|30110|6|Mentioned|p81|||See also p85. Cretaceous age.||||||07-OCT-20
20259|Winning Group|30365|6|Mentioned|Fig.8|||||||||
20259|Winning Group|30693|6|Mentioned|p50|||||||||
20259|Winning Group|31083|6|Mentioned|p455|||||||||
20259|Winning Group|31561|6|Mentioned|p38|||Early to Late Cretaceous||||||
20259|Winning Group|31604|5|Briefly described|p6|||Neocomian to Coniacian. See also Table 4. Units listed||||||
20259|Winning Group|31738|6|Mentioned|p59|||||||||
20259|Winning Group|32166|6|Mentioned|Fig.2|||||||||
20259|Winning Group|32648|6|Mentioned|p32|||Cretaceous||||||
20259|Winning Group|32711|6|Mentioned|Fig.3|||||||||
20259|Winning Group|32715|6|Mentioned|Fig.16|||||||||
20259|Winning Group|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
20259|Winning Group|33386|6|Mentioned|Fig.7|||||||||
20259|Winning Group|33450|6|Mentioned|Fig.3|||||||||
20259|Winning Group|33453|4|Described|p72|||||||||
20259|Winning Group|33813|6|Mentioned|p7|||See also Figs 5 & 6||||||
20259|Winning Group|34840|6|Mentioned|p66|||||||||
20259|Winning Group|34841|6|Mentioned|Fig.5|||||||||
20259|Winning Group|35105|6|Mentioned|Fig.5|||||||||
20259|Winning Group|35144|6|Mentioned|Fig.3|||||||||
20259|Winning Group|35282|6|Mentioned|Fig.2|||||||||
20259|Winning Group|36257|6|Mentioned|Table 2.1|||||||||
20259|Winning Group|36293|6|Mentioned|p165|||||||||
20259|Winning Group|36890|3|Fully described|p295|||Formerly Winning Series.||||||14-NOV-07
20259|Winning Group|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20259|Winning Group|37320|6|Mentioned|p235|||||||||
20259|Winning Group|37360|5|Briefly described|p573|||||||||
20259|Winning Group|37422|6|Mentioned|p15|||||||||
20259|Winning Group|38485|4|Described|p14|||||||||
20259|Winning Group|39158|5|Briefly described|p36|||||||||
20259|Winning Group|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
20259|Winning Group|39211|6|Mentioned|p60|||||||||
20259|Winning Group|39427|6|Mentioned|p12|||||||||
20259|Winning Group|39486|6|Mentioned|p2092|||||||||
20259|Winning Group|40340|5|Briefly described|p14|||||||||
20259|Winning Group|40343|5|Briefly described|p11|||||||||
20259|Winning Group|40877|5|Briefly described|p53|||||||||
20259|Winning Group|41172|6|Mentioned|p116|||||||||
20259|Winning Group|41271|3|Fully described|p146|||||||||
20259|Winning Group|41436|6|Mentioned|Fig.6|||||||||
20259|Winning Group|41438|4|Described|p109|||||||||
20259|Winning Group|41440|4|Described|p137|||||||||
20259|Winning Group|41441|6|Mentioned|Fig.6|||||||||
20259|Winning Group|41446|5|Briefly described|p203|||||||||
20259|Winning Group|41729|6|Mentioned|Fig.2|||||||||
20259|Winning Group|41732|6|Mentioned|p534|||See also Fig.3||||||
20259|Winning Group|42116|5|Briefly described|p10|||||||||
20259|Winning Group|42598|4|Described|p95|||||||||
20259|Winning Group|42613|4|Described|p95|||||||||
20259|Winning Group|42615|6|Mentioned|p35|||||||||
20259|Winning Group|42673|6|Mentioned|p194|||||||||
20259|Winning Group|43564|6|Mentioned|p445|Barremian|Valanginian|||||||
20259|Winning Group|43598|6|Mentioned|p813|||||||||
20259|Winning Group|43710|6|Mentioned|p31|||||||||
20259|Winning Group|43712|5|Briefly described|p11|||||||||
20259|Winning Group|43722|5|Briefly described|p10-11||Valanginian|||||||
20259|Winning Group|43724|5|Briefly described|p29|||||||||
20259|Winning Group|44344|14|Not recorded|p.17-18,22,opp.4,map||Cretaceous|Cret.; includes Birdrong Formation, Muderong Shale, Windalia Radioarite & Gearle Siltstone (top). (G50-1).||||||
20259|Winning Group|44345|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
20259|Winning Group|44532|4|Described|p.8, map|||(G50-5).||||||
20259|Winning Group|44533|5|Briefly described|map legend||Early Cretaceous|Lower Cretaceous.||||||
20259|Winning Group|44537|14|Not recorded|map legend|||Lower-Upper Cretaceous.||||||
20259|Winning Group|44657|14|Not recorded|p.11,12|||||||||
20259|Winning Group|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Includes Wogatti Sandstone, Birdrong Formation, Muderong Shale, Windalia Radiolarite, Thirindine Formation, Gearle Siltstone and Alinga Formation.||||||04-MAY-07
20259|Winning Group|45016|14|Not recorded|p163|||||||||
20259|Winning Group|45142|6|Mentioned|p8|||||||||
20259|Winning Group|46808|6|Mentioned|Table 2|||Offshore||||||
20259|Winning Group|46950|6|Mentioned|Fig.15|||||||||
20259|Winning Group|48610|14|Not recorded|p14|||Salt Marsh area.||||||
20259|Winning Group|48858|14|Not recorded|p.5,6|||(G50-1/Norton).||||||
20259|Winning Group|48861|14|Not recorded|p.5|||Ref.Condon et al 1956.||||||
20259|Winning Group|49942|5|Briefly described|p4 Fig.3, p11|Late Cretaceous|Early Cretaceous|Overlain by Haycock Marl (unconformably) and Toolonga Calcilutite (disconformably). Max. thickness: 600 m. Geological Province: Gascoyne Platform.||||||
20259|Winning Group|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin (Barrow Sub-basin).||||||
20259|Winning Group|60118|6|Mentioned|p29|||Mentioned only in terms of Winning Group shales (referring to Muderong Shale and Gearle Siltstone. Geological Province: Barrow Sub-basin, North Carnarvon Basin.||||||
20259|Winning Group|60384|5|Briefly described|p244, p243 Fig 2a, p259|Cretaceous|Early Cretaceous|Southern Carnarvon Basin. Silty and pelagic rocks from a marine transgression.|||Includes Birdrong Sandstone, Muderong Shale, Windalia Radiolarite, Gearle Siltstone|Overlain by Haycock Marl in places and disconformably overlain by Toolonga Calcilutite in places|Basal sandstone overlain by marine shale and radiolarite|
20259|Winning Group|61563|5|Briefly described|p576|Early Cretaceous|Early Cretaceous|See also p579 Fig. 3, p584.||||||
20259|Winning Group|61811|5|Briefly described|p3 Fig.2, p8, p11, pp13-17.|Cenomanian|Barremian|Northern Perth Basin.|||Includes Birdrong Sandstone, Windalia Sandstone Member and Windalia Radiolarite, Muderong Shale, Alinga Formation and Gearle Siltstone.|||
20259|Winning Group|61958|5|Briefly described|Map sheets 1 and 2|Early Cretaceous|Early Cretaceous|Includes: Birdrong Formation, Muderong Shale, Windalia Radiolarite, Thirindine Formation, Gearle Siltstone and Alinga Formation.||||||21-MAR-06
20259|Winning Group|63068|5|Briefly described|p44 Figs. 1, 2|Cenomanian|Aptian|Includes Windalia Radiolarite and Gearle Siltstone. Geological Province: Carnarvon Basin.||||||27-FEB-07
20259|Winning Group|64580|4|Described|map legend|Late Cretaceous|Early Cretaceous|Undivided; shale, siltstone, marl, and basal sandstone; commonly glauconitic; includes BIRDRONG SANDSTONE, MARDIE GREENSAND, MUDERONG SHALE, ALINGA FORMATION (in south), WINDALIA RADIOLARITE, GEARLE SILTSTONE, and HAYCOCK MARL (in north).||||||09-DEC-08
20259|Winning Group|64635|5|Briefly described|p4 Fig.3, p7  |Cenomanian|Barremian||||Includes the Birdrong Sandstone, Muderong Shale, Windalia Radiolarite, Gearle Siltstone and Alinga Formation.|||
20259|Winning Group|64973|4|Described|p504, p504 Fig. 2, p505 Fig. 3|Early Cretaceous|Early Cretaceous|Includes; Birdrong Sandstone, Mardie Greensand, Muderong Shale, Windalia Radiolarite, Windalia Sandstone and Gearle Siltstone. Transgressive siliciclastic succession that was deposited in mostly open marine-shelf conditions. Also on p506 Fig. 4.||||||
20259|Winning Group|67200|6|Mentioned|p17 table 1||||||Includes Gearle Siltstone, Alinga Formation, Windalia Radiolarite, Muderong Shale, Mardie Greensand Member, Birdrong Sandstone|||
20259|Winning Group|67340|6|Mentioned|p6|Late Cretaceous|Early Cretaceous|Northern Perth Basin.|||Birdrong Sandstone, Windalia Radiolarite, Alinga Formation, Gearle Siltstone.|||
20259|Winning Group|67970|5|Briefly described|p25 Fig.4.|Cenomanian|Hauterivian|Exmouth Plateau.|||Includes Muderong Shale, Windalia Radiolarite and Gearle Siltstone.|||
20259|Winning Group|69011|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||Includes the Birdrong Sandstone.||Includes fine- to coarse-grained sandstone; locally silty; commonly poorly consolidated; locally glauconitic.|
20259|Winning Group|69166|5|Briefly described|500k_geologyp08_lut.csv|Cretaceous|Cretaceous||||Includes Birdrong Sandstone, Mardie Greensand, Muderong Shale, Windalia Radiolarite, Gearle Siltstone, Haycock Marl, Alinga Formation||Shale, siltstone, marl and basal sandstone; commonly glauconitic.|
20259|Winning Group|69182|6|Mentioned|Ch2 p3, Ch3 p3, Ch3 p30|Early Cretaceous|Early Cretaceous|Perth Basin.|||Includes the Birdrong Sandstone.|||
20259|Winning Group|69185|4|Described|GEOL_LUT_CSV files|Late Cretaceous|Early Cretaceous|Of Northern Carnarvon Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||Includes Alinga Formation, Birdrong Sandstone, Gearle Siltstone, Haycock Marl, Mardie Greensand, Muderong Shale, Windalia Radiolarite.||Undivided; shale, siltstone, marl, and basal sandstone; commonly glauconitic.|
20259|Winning Group|69297|4|Described|p247, p249|Barremian|Hauterivian|Southern Carnarvon Basin. A fining upwards sequence deposited in a marine setting during a transgressive cycle.|||Includes the Birdrong Sandstone, Muderong Shale, Windalia Radiolarite and the Gearle Siltstone.|Unconformably overlies the Woodleigh Formation. Unconformably overlain by the Haycock Marl.|Sandstone and shale.|
20259|Winning Group|69583|5|Briefly described|p130, Plate 3.|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||||Shale, siltstone, marl, and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20259|Winning Group|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Coniacian|Valanginian|See also Regional: Fig.6. Northern Carnarvon Basin.|||Birdrong Sandstone, Muderong Shale, Windalia Radiolarite, Gearle Siltstone and Haycock Marl.|Overlies Forestier Claystone. Is overlain by Toolonga Calcilutite.||
20259|Winning Group|70127|5|Briefly described|Map legend|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||||Shale, siltstone, marl and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20259|Winning Group|70138|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Southern Carnarvon Basin.|||||Shale, siltstone, marl and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20259|Winning Group|70795|4|Described|100k_geologyp_lut.csv|Santonian|Valanginian|Also 100k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv|140-83 Ma||Includes Birdrong Sandstone||Shale, siltstone, marl, and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20259|Winning Group|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Carnarvon Basin.||||||
20259|Winning Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, radiolarite, sandstone, shale|
20259|Winning Group|71273|5|Briefly described|Map legend.|Cretaceous|Cretaceous||140-85 Ma.||||Shale, siltstone, marl and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20259|Winning Group|72034|5|Briefly described|500k_interpgeop16_lut|Santonian|Valanginian|Northern Carnarvon Basin; Southern Carnarvon Basin.  Age from biostratigraphy.|||||Shale, siltstone, marl, and basal sandstone; commonly glauconitic; radiolarian siltstone in central part.|
20285|Wirara Formation|22496|6|Mentioned|p11||Neoproterozoic|Kuniandi Group||||||
20285|Wirara Formation|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Kuniandi Group.||||||
20285|Wirara Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20285|Wirara Formation|32660|5|Briefly described|Table 6|||||||||
20285|Wirara Formation|32728|6|Mentioned|Fig.16|||See also Table 7||||||
20285|Wirara Formation|36551|6|Mentioned|Table 10|||||||||
20285|Wirara Formation|36888|4|Described|p215|||||||||
20285|Wirara Formation|36898|5|Briefly described|Table III|||||||||
20285|Wirara Formation|37927|6|Mentioned|p511|||||||||
20285|Wirara Formation|38157|6|Mentioned|Table X|||||||||
20285|Wirara Formation|41405|6|Mentioned|p206|||||||||
20285|Wirara Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount Ramsay area. 450-490 m thick.||Kuniandi Group||Conformably overlies Stein Formation. Overlain by Mount Bertram Sandstone conformably.|Thin-bedded siltstone and shale, interbedded fine sandstone; green and red-brown banded siltstone and fine sandstone near base.|
20285|Wirara Formation|44231|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Of the Kuniandi Group. Green to grey laminated shale and siltstone, purple siltstone, and green and purple sandstone.  Age: c.610Ma. Geological Province: Louisa Basin.||||||19-MAY-05
20285|Wirara Formation|44397|14|Not recorded|p.15,16, Table 3||Adelaidean|Kuniandi Group. Defn. on Tech.File E/52-9.||||||
20285|Wirara Formation|44398|14|Not recorded|map legend||Adelaidean|||||||
20285|Wirara Formation|45047|4|Described|p36|||Kuniandi Group||||||
20285|Wirara Formation|48927|2|Defined|p14|Adelaidean|Adelaidean|||||||
20285|Wirara Formation|63458|6|Mentioned|p873 Fig.2, p881, p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Kuniandi Group.||Overlies Landrigan Tillite.||
20285|Wirara Formation|67484|6|Mentioned|p294 Tb.1|Ediacaran|Ediacaran|Mount Ramsay area, West Kimberley.||Of the Kuniandi Group.||Overlain by the Mount Bertram Sandstone. Underlain by the Stein Formation.||
20285|Wirara Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Mount Ramsay area, Kimberley region.||Kuniandi Group.||Overlies Stein Formation. Is overlain by Mount Bertram Sandstone.||
20285|Wirara Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Kuniandi Group.||||
20285|Wirara Formation|68244|4|Described|p660,665-666|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region.||Unit of Kuniandi Group.||Overlain by mount Bertram Sandstone. Underlain by Stein Formation and Landrigan Formation.|Green-purple laminated siltstone|
20285|Wirara Formation|68473|6|Mentioned|p531|||Mount Ramsay.||Kuniandi Group||Equivalent to the Egan Formation.||
20285|Wirara Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Kuniandi Group.|||Green to grey fissile to thinly flaggy laminated shale and siltstone with pyrite in places, purple siltstone, and green and purple sandstone interbeds|
20298|Wirraway Formation|41199|2|Defined|p15|early Quaternary|late Tertiary|Reserved as Wirraway||||||
20307|Wirrildar beds|23282|6|Mentioned|p72|||May correlate with Observatory Hill Formation. of central Officer Basin.||||||
20307|Wirrildar beds|23288|6|Mentioned|Fig.5|||||||||
20307|Wirrildar beds|31969|3|Fully described|p8|||See also P9-10||||||
20307|Wirrildar beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
20307|Wirrildar beds|43052|5|Briefly described|Table 2.1|||||||||
20307|Wirrildar beds|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||25-MAY-05
20307|Wirrildar beds|43258|5|Briefly described|Map Legend||Cambrian|||||||
20307|Wirrildar beds|43298|5|Briefly described|Map Legend||Cambrian|||||||
20307|Wirrildar beds|44133|5|Briefly described|p39, 42, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Overlies: Punkerri Sandstone (un). Underlies: Kulyong Volcanics (un).||||||07-NOV-08
20307|Wirrildar beds|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||
20307|Wirrildar beds|61108|5|Briefly described|map legend|Cambrian|Cambrian|Feldspathic sandstone, siltstone and dolomite.||||||
20307|Wirrildar beds|61732|6|Mentioned|p79|Cambrian|Cambrian|Geological Province: Birksgate Sub-basin.||||||07-FEB-11
20307|Wirrildar beds|65416|5|Briefly described|p144.|||Correlated with McFadden Formation. Written as Wirrildar Beds on p144.||||Overlies Punkerri Sandstone. Is unconformably overlain by Kulyong Volcanics and Table Hill Volcanics.||
20307|Wirrildar beds|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as Em5.|||||Mostly non-marine sandstone, siltstone, claystone and minor dolomite, limestone, chert and conglomerate.|
20307|Wirrildar beds|67921|5|Briefly described|Map legend|Cambrian|Cambrian|Grouped with Arcoeillina Sandstone and Observatory Hill Formation. Group description: Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.||||||
20307|Wirrildar beds|69091|5|Briefly described|p35|||Predates Late Cambrian Table Hill Volcanics, suggests gentle folding is due to Delamerian Orogeny.|||||Thick, gently folded sandstone succession.|
20307|Wirrildar beds|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Cambrian|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.|541-509 Ma (inferred)||||Fine grained, micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards|
20307|Wirrildar beds|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Officer Basin.||||||
20307|Wirrildar beds|71146|5|Briefly described|p6, p21|Cambrian|Neoproterozoic|Officer Basin.||||Unconformably overlain by the Table Hill Volcanics.|Sandstone.|
20307|Wirrildar beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||arkose|
20307|Wirrildar beds|71268|4|Described|GEOL_LUT_CSV files|Series 2|Cambrian|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 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|541-511 Ma (inferred)|Unit of Marla Group.|||Fine-grained micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards|
20307|Wirrildar beds|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Cambrian|Officer Basin (Phase 1).|||||Fine grained, micaceous sandstone and dolomite, with basal arkosic sandstone; fines and becomes more calcareous upwards.|
20307|Wirrildar beds|73100|5|Briefly described|Map legend|Cambrian|Cambrian|Subsurface. Mapped as one unit with Arcoeillina Sandstone and Observatory Hill Formation.||||||
20307|Wirrildar beds|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Mapped as one unit with Arcoeillina Sandstone and Observatory Hill Formation. Subcrop and minor outcrop.|||||Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.|
20324|Wittecarra Sandstone|12729|5|Briefly described|p.15||Triassic|Outcrops in coastal cliffs at Shell House, south of Kalbarri as 11 m of poorly consolidated sandstone. See also reference to mis-named Wittecarra Formation p28.||||Overlies the Tumblagooda Sandstone.||
20324|Wittecarra Sandstone|14228|5|Briefly described|p5 Fig.2, p8, p19|Triassic|Triassic|Type section 11 m thick at Shell House, in coastal cliffs south of Kalbarri.||||Overlies Tumblagooda Sandstone. Overlain (conformably) by Kockatea Shale.||06-OCT-16
20324|Wittecarra Sandstone|23279|6|Mentioned|p18|||||||||
20324|Wittecarra Sandstone|23520|5|Briefly described|p9, p6 Fig. 4|Permian|Permian|Unconformable over Tumblagooda Sst. in Caranarvon Basin area; unconformably overlies Carynginia Fm. in the Abrolhos Sub-basin.  Type section in Carnarvon Basin.  Sealed by overlying Kockatea Shale.  Contains Early Permian and Early Triassic palynmorphs.||||||
20324|Wittecarra Sandstone|23726|4|Described|p15|Early Triassic|Early Triassic|Overlain by Kockatea Shale. Underlain by Tumblagooda Sandstone. Geological Province: Carnarvon Basin.||||||28-APR-09
20324|Wittecarra Sandstone|23815|4|Described|p290|Early Triassic|Early Triassic|Geological Province: Carnarvon Basin. Overlain by Kockatea Shale (conformable). Underlain by Tumblagooda Sandstone. Max. thickness: 9 m.||||||28-APR-09
20324|Wittecarra Sandstone|24351|5|Briefly described|Plate 4 (in pocket)|Early Triassic|Early Triassic|Geological Province: Gascoyne Platform/Sub-basin.||||||13-DEC-07
20324|Wittecarra Sandstone|24443|5|Briefly described|Fig.30|Early Triassic|Early Triassic|Unconformably overlies Carynginia Formation and Irwin River Coal Measures. Overlain by and interfingers with Kockatea Shale. Geological Province: Bight Basin.||||||03-FEB-05
20324|Wittecarra Sandstone|36257|6|Mentioned|Table 2.1|||||||||
20324|Wittecarra Sandstone|36890|3|Fully described|p290|||Formerly Wittecarra Formation.||||||05-FEB-08
20324|Wittecarra Sandstone|38998|4|Described|p19|||||||||
20324|Wittecarra Sandstone|40340|5|Briefly described|p14|||||||||
20324|Wittecarra Sandstone|40341|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
20324|Wittecarra Sandstone|40617|6|Mentioned|p18|||||||||
20324|Wittecarra Sandstone|41172|6|Mentioned|p124|||||||||
20324|Wittecarra Sandstone|41271|3|Fully described|p116|||||||||
20324|Wittecarra Sandstone|42116|5|Briefly described|p10|||||||||
20324|Wittecarra Sandstone|49942|5|Briefly described|p4 Fig.3|Early Triassic|Late Permian|Conformably overlain by Kockatea Shale. Geological Province: Gascoyne Platform.||||||
20324|Wittecarra Sandstone|60384|5|Briefly described|p244, p243 Fig 2a|Early Triassic |Late Permian|Perth Basin.||||||
20324|Wittecarra Sandstone|61811|5|Briefly described|p3 Fig.2, p8, pp17-19.|Early Triassic|Early Triassic|Northern Perth Basin. Derived from underlying Tumblagooda Sandstone.||||Disconformably overlies Tumblagooda Sandstone. Is overlain by Kockatea Shale.|Basal conglomerate, then silty sandstone and siltstone, sandstone, conglomerate, and capped by sandstone with probable plant rootlets.|
20324|Wittecarra Sandstone|64635|5|Briefly described|p4 Fig.3, p7, p14, p15 Fig.13   |Olenekian|Induan|p14, diagrams and photos of the type section at Shell House, 11 km S of Kalbarri. Derived from underlying Tumblagooda Sandstone.||||Disconformably overlies the Tumblagooda Sandstone. Underlies the Kockatea Shale.|Consists of a basal conglomerate, overlain in turn by silty sandstone and siltstone, sandstone, conglomerate, and capped by a sandstone with probable plant rootlets.|
20324|Wittecarra Sandstone|67340|6|Mentioned|p6|Early Triassic|Early Triassic|Northern Perth Basin.||||||
20324|Wittecarra Sandstone|67370|6|Mentioned|p318 Fig.10.|Changhsingian|Changhsingian|Northern Perth Basin.||||||
20324|Wittecarra Sandstone|69182|6|Mentioned|Ch3 p12-p13|||Perth Basin.||||Overlain by the Kockatea Shale.||
20324|Wittecarra Sandstone|70097|5|Briefly described|p20 Fig.4|Changhsingian|Changhsingian|Northern Perth Basin. Dongara Saddle and Dandaragan Trough.||||Overlies Dongara or Wagina Sandstones. Is overlain by Kockatea Shale.|Sandstone, and ?siltstone.|12-SEP-17
20327|Wittenoom Formation|22682|6|Mentioned|p29|||Carrawine Supersequence||||||
20327|Wittenoom Formation|22689|6|Mentioned|137,138 fig 1,139|||Of Hamersley Group, Hamersley Basin. Underlying unit Marra Mamba Formation. Also on page 141 fig 2||||||
20327|Wittenoom Formation|22701|4|Described|p40|Siderian|Archean|Also Fig2,p39. 2541 +/- 32 Ma. Overlies Marra Mamba Iron Formation, overlain by Mount Sylvia Formation.||||||07-NOV-08
20327|Wittenoom Formation|23045|5|Briefly described|289|||Parent Hamersley Group||||||
20327|Wittenoom Formation|23046|5|Briefly described|171|||||||||
20327|Wittenoom Formation|23127|5|Briefly described|p376|||||||||
20327|Wittenoom Formation|23280|5|Briefly described|Table1p1085||Archean|Max Age: 2561 (+/-) 8 Ma.||||||07-NOV-08
20327|Wittenoom Formation|23354|5|Briefly described|315|||||||||
20327|Wittenoom Formation|23536|5|Briefly described|Fig 2 p 429|||||||||
20327|Wittenoom Formation|23570|5|Briefly described|p14|||Of Hamersley Group.   Geological Province: Pilbara Craton||||||
20327|Wittenoom Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Underlying unit Marra Mamba Iron Formation.||||||07-NOV-08
20327|Wittenoom Formation|23612|6|Mentioned|p843|||||||||
20327|Wittenoom Formation|23746|5|Briefly described|p21|||Formerly Wittenoom Dolomite.||||||
20327|Wittenoom 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
20327|Wittenoom Formation|23890|5|Briefly described|p9|Paleoproterozoic|Archean|Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
20327|Wittenoom Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.56 Ga. Geological Province: Pilbara Craton. Parent: Hamersley Group. Overlying Unit: Mount Sylvia Formation. Underlying Unit: Marra Mamba Formation.||||||07-NOV-08
20327|Wittenoom Formation|24041|5|Briefly described|p495|Archean|Archean|||||||07-NOV-08
20327|Wittenoom Formation|24231|5|Briefly described|p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
20327|Wittenoom Formation|24426|6|Mentioned|p243 Fig.13|||See also Wittenoom Dolomite.||||||07-FEB-11
20327|Wittenoom Formation|24533|5|Briefly described|p5 Table 2|Archean|Archean|Of the Hamersley Group. Conformably overlies the Marra Mamba Iron Formation. Age: 2561 +/- 8Ma (crystal rich tuff).||||||07-NOV-08
20327|Wittenoom Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Hamersley Group. Overlies Marra Mamba Iron Formation. Overlain by Mount Sylvia Formation. Dolomite. Geological Province: Hamersley Basin.||||||07-NOV-08
20327|Wittenoom Formation|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton||||||
20327|Wittenoom Formation|41622|6|Mentioned|Fig.2|||||||||
20327|Wittenoom Formation|43063|6|Mentioned|p49|||Acknowledgement given that Wittenoom Dolomite is superseded||||||
20327|Wittenoom Formation|43064|4|Described|p68|||Supersedes Wittenoom Dolomite.||||||23-MAR-09
20327|Wittenoom Formation|43262|5|Briefly described|Map Legend||Archean|of Hamersley Group.||||||07-NOV-08
20327|Wittenoom Formation|43290|5|Briefly described|p6||Archean|of Hamersley Group. Supersedes Wittenoom Dolomite.||||||07-NOV-08
20327|Wittenoom Formation|43644|6|Mentioned|Fig.4,p591|||||||||
20327|Wittenoom Formation|43673|6|Mentioned|p374|||Ejecta age: approx. 2.6 Ga||||||
20327|Wittenoom Formation|50549|6|Mentioned|p1159|||||||||
20327|Wittenoom Formation|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersly Group. Includes Bee George and Paraburdoo Members. Overlian by Mount Sylvia Formation, underlain by Marra Mumba Iron Formation.||||||
20327|Wittenoom Formation|60706|5|Briefly described|p623, p643 App.1|Archean|Archean|Of the Hamersley Group. Includes West Angela, Paraburdoo and Bee Gorge Members. Overlain by Mount Sylvia Formation. Age: 2561+/-8 Ma (SHRIMP). Geological Province: Hamersley Basin.||||||07-NOV-08
20327|Wittenoom Formation|61265|6|Mentioned|p46-47 Fig.2|||Geological Province: Pilbara Craton.||||||
20327|Wittenoom Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Hamersley Group. Dolomite, dolomitic mudstone, chert and volcanic sandstone.||||||
20327|Wittenoom Formation|61560|5|Briefly described|p498 Tb. 4|||Includes the Bee Gorge Member. Geological Province: Hamersley Basin.||||||
20327|Wittenoom Formation|61575|5|Briefly described|p759|Neoarchean|Neoarchean|Includes the Paraburdoo Member, a thick accumulation of carbonate. Geological Province: Hamersley Basin.||||||07-NOV-08
20327|Wittenoom Formation|61576|5|Briefly described|p773|||Of the Hamersley Group. Contains Neoarchaean impact spherules in its Bee Gorge Member. Geological Province: Hamersley Basin.||||||
20327|Wittenoom Formation|62129|3|Fully described|p9|Archaean|Archaean|Formerly Wittenoom Dolomite. Of Hamersley Group. Includes West Angela, Paraburdoo and Bee Gorge Members. Thickness: 700m. Geological Province: Hamersley Basin.||||||14-FEB-11
20327|Wittenoom Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Metamorphosed thin- to medium-bedded dolomite, dolomitic pelite, chert, and volcanic sandstone.||||||
20327|Wittenoom Formation|63153|6|Mentioned|p1359-1360, p1361 Fig.2, p1363, p1368 |||Typically deeply eroded; mature karst topography, largely buried by Tertiary to Recent valley fill sediments.||Unit in Hamersley Group.|Includes West Angela Member.|Overlies Marra Mamba Iron Formation. Is overlain by Mount Sylvia Formation.||
20327|Wittenoom Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Hamersley Group. Geological Province: Hamersley Basin. Thin to medium bedded dolomite, dolomitic mudstone, chert and volcanic sandstone. Underlies: Mount Mcrae Shale and Mount Sylvia Formation. Overlies: Marra Mamba Iron Formation. Age: 2561Ma.||||||07-NOV-08
20327|Wittenoom Formation|63432|5|Briefly described|p736 Fig. 2 and Fig. 3, p751|Proterozoic|Proterozoic|Produces 'terra rossa' soils.||||||07-FEB-11
20327|Wittenoom Formation|64580|4|Described|map legend||Neoarchean|Of Lower Hamersley Group. Thin- to medium-bedded dolomite, dolomitic mudstone, chert, and felsic to mafic volcanic sandstone; metamorphosed.||||||09-DEC-08
20327|Wittenoom Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Hamersley Group. Age: 2561-2541Ma.  Geological Province: Hamersley Basin. Thinly bedded dolomite, black chert, shale, and sandstone.||||||
20327|Wittenoom Formation|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
20327|Wittenoom Formation|65683|5|Briefly described|p801 Fig2, p802|||Of Hamersley Group. Underlies Mount Sylvia Formation; overlies Mount Newman Member of Marra Mamba Iron Formation. Includes West Angela Member. See also Wittenoom Dolomite p799. Correlated with Carawine Dolomite.||||||08-MAR-12
20327|Wittenoom Formation|65757|6|Mentioned|p81 Tb.2, p84 Fig.2, p87 Fig.7, p88|||in the Hamersley Group. Includes Bee Gorge Member. Underlies the [Mount] Sylvia Formation.||||||
20327|Wittenoom Formation|65825|5|Briefly described|p23.|||A westerly correlative of the Carawine Dolomite.||Unit in lower part of Hamersley Group.|||Dolomitic rocks.|
20327|Wittenoom Formation|65829|5|Briefly described|p25.|Neoarchean|Neoarchean|Formerly Wittenoom Dolomite; redefined in 1993. Hamersley Ranges. Contains a similar horizon to the chaotic spherule-bearing megabreccia in the Carawine Dolomite, interpreted as evidence of an asteroid impact in an oceanic environment.|c.2561 Ma (Trendall et al. 1998).||Includes Bee Gorge Member.|||
20327|Wittenoom Formation|67056|5|Briefly described|p419 Fig.2, p439, p445. |||In various ore-concentrating models, this unit is seen as the source of alkaline hypogene solutions into the ore zones.||Unit in Hamersley Group.||Overlies Marra Mamba Iron Formation. Is overlain by Mount Sylvia Formation.|Includes dolomite.|
20327|Wittenoom Formation|67130|6|Mentioned|p3 fig 2, p24 fig 17|||Also referred to as Wittenoom Dolomite which is outdated (p8 fig 5)||Hamersley Group|Includes West Angela Member, Paraburdoo Member, Bee Gorge Member|Overlies Marra Mamba Iron Formation, overlain by Mount Sylvia Formation||
20327|Wittenoom Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Formerly Wittenoom Dolomite (see p643). Present in the Southern Pilbara.||Hamersley Group||||
20327|Wittenoom Formation|67201|4|Described|p34, p51-53, p55|||Visible at base of Hamersley Range Escarpment. Shallow-water deposits. Shown as Wittenoom Dolomite on p53 Fig.40.|c. 2560 Ma|Hamersley Group|West Angelas Member, Paraburdoo Member, Bee Gorge Member|Is overlain by Mount Sylvia Formation. Overlies Marra Mamba Iron Formation. Lateral equivalent of Carawine Dolomite.|Carbonate-dominated.|25-NOV-16
20327|Wittenoom Formation|67721|5|Briefly described|p38 Fig.9|Neoarchean|Neoarchean||c. 2553 Ma|Of the Hamersley Group.|Includes Bee Gorge Member, Paraburdoo Member, and West Angela Member.|||
20327|Wittenoom Formation|67827|6|Mentioned|p415, p429, p432|||Microstructure of iron ores discussed.|||||Dolomite.|
20327|Wittenoom Formation|67829|5|Briefly described|pp447-448, pp452-454.|||Hamersley Basin. Equivalent of Carawine Dolomite in East Pilbara. Called the Wittenoom Dolomite on pp447-448.||||Overlies the Marra Mamba Iron Formation.||
20327|Wittenoom Formation|68035|4|Described|p292, Fig 6|Neoarchean|Neoarchean|Hamersley Basin. Carbonate dominated.||Of Hamersley Group.|Includes West Angela Member, Paraburdoo Member, Bee Gorge Member.|Separates the Marra Mamba (underlying) and Brockman (overlying) iron formations.|Shale, carbonate.|
20327|Wittenoom Formation|68280|6|Mentioned|p5, p41, p54, p62|Neoarchean|Neoarchean|Wittenoom Dolomite also used (p62 fig 67).|2560-2500 Ma|Hamersley Group|Includes Bee Gorge Member, Paraburdoo Member, West Angela Member|Overlain by Mount Sylvia Formation, overlies Marra Mamba Iron Formation||18-JAN-23
20327|Wittenoom Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Hamersley Basin.||Of the Hamersley Group.|||Thinly bedded dolomite, with minor black chert, shale and sandstone; metamorphosed.|06-MAY-14
20327|Wittenoom Formation|69080|6|Mentioned|p687|||||Unit in Hamersley Group.||Overlies Marra Mamba Iron Formation. Is overlain by Mount Sylvia Formation.||
20327|Wittenoom Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Thin- to medium-bedded dolomite, dolomitic mudstone, chert, and felsic to mafic volcanic sandstone; metamorphosed.|
20327|Wittenoom Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Thinly bedded dolomite, with minor black chert, shale, and sandstone|
20327|Wittenoom Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northwest and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Hamersley Group.|||Thin- to medium-bedded dolomite, dolomitic mudstone, chert, and felsic to mafic volcanic sandstone; metamorphosed|
20327|Wittenoom Formation|69538|5|Briefly described|p517 Fig.3, p520, p523, p526|Paleoproterozoic|Paleoproterozoic|See also p528-530, p532 Tb.3, p534-535, p552, p555, p565, p571-572, p574-576, p578 Fig.47, p583-585. Includes part of what the authors call the Fortescue Reef limestone.||Unit in Hamersley Group.|Includes West Angela, Paraburdoo and Bee Gorge Members.||Includes shallow-water reef limestones.|
20327|Wittenoom Formation|69563|5|Briefly described|p690 Tb.1, p696|||Hamersley Basin. Contains two spherule marker beds.|2561 +/- 8 Ma.||Includes Bee Gorge and Paraburdoo  Members.|||
20327|Wittenoom Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Hamersley Group.||||
20327|Wittenoom Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|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. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2597-2504 Ma (isotopic; inferred)|Unit of Hamersley Group.|||Thinly bedded dolomite, with minor black chert, shale, and sandstone|
20327|Wittenoom Formation|69739|5|Briefly described|p69-76|||Hamersley Basin. Source(s) of high Sr-87 concentrations in deep groundwater are discussed.||Hamersley Group.||Overlies Marra Mamba Iron Formation. Is overlain by Mount Sylvia Formation.|Dominantly dolomite and shale. Water-bearing.|
20327|Wittenoom Formation|69745|6|Mentioned|p272-273, 276, 278-283, 287-288, 290|||Crops out in the Mount Wall Fe deposit area, Hamersley Province.||Hamersley Group.|Paraburdoo Member.||Carbonates and shales.|
20327|Wittenoom Formation|70733|6|Mentioned|p116||||||Spherule Marker Bed.|||
20327|Wittenoom Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2597-2504 Ma||||Thinly bedded dolomite, with minor black chert, shale and sandstone.|
20327|Wittenoom Formation|71042|5|Briefly described|p64 fig 1, p65, p66|Archean|Archean|See also p72-p73, p75, p95.||Hamersley Group|||Dolomite.|28-MAY-19
20327|Wittenoom Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||chert, shale, volcaniclastic rock, dolostone|
20327|Wittenoom Formation|71513|6|Mentioned|p66,|||Pilbara Craton. Interpreted to have been deposited on a continental shelf.||Hamersley Group||Overlies the Marra Mamba Iron Formation.|Turbidites and carbonates.|
20327|Wittenoom Formation|71550|6|Mentioned|p45|||Geological province: Of Hamersley Basin.||Unit of Hamersley Group.|Includes Bee Gorge Member.|||03-SEP-19
20327|Wittenoom Formation|71808|5|Briefly described|p2, p6, p21, p38-p39|||Hamersley Province. See also p52, p81, p117, p127, p149-p150, p156, p192, p199.|||Includes the Paraburdoo Member, West Angela Member and the Bee Gorge Member.|||
20327|Wittenoom Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Hamersley Basin.|max age 2597+/-5 Ma, min ~2504 Ma.|Hamersley Group, lower|||Thinly bedded dolomite and dolomitic shale, with minor black chert, shale, banded iron formation and sandstone.|
20327|Wittenoom Formation|72447|6|Mentioned|p240-242||||||West Angela Member, Paraburdoo Member|||
20327|Wittenoom Formation|72493|6|Mentioned|p29-30|Archaean|Archaean|Hamersley Basin.||||||
20327|Wittenoom Formation|72569|5|Briefly described|p1-3, p5, p16, p19-20, p22|||Of the Hamersley Basin. Average accumulation rate of 2.5m.Ma. Roll-up structures in this formation are attributed to microbial mat activity.||Hamersley Group|Includes West Angela Shale Member, Paraburdoo Member, Bee Gorge Member, in ascending order.|||
20327|Wittenoom Formation|72570|6|Mentioned|p3 fig 1|||||Hamersley Group||||
20327|Wittenoom Formation|72712|5|Briefly described|p9 Fig.5, p10, p11 Fig.8.|Neoarchean|Neoarchean|Detailed description as part of the Hamersley Group given by Martin et al. (2000), Martin and Morris (2010). Shown as Wittenoom Dolomite p7, 10.|c. 2597 Ma to c. 2565 Ma.|Hamersley Group||Conformably overlies Marra Mamba Iron Formation and underlies Mount Sylvia Formation.|Includes dolomite.|
20327|Wittenoom Formation|73022|4|Described|p2-3, p4 Fig.3-4, p5 Fig.5-6, p6 Fig.8|||Siliciclastic and carbonate beds represent distal turbidites and hemi-pelagites deposited on a deep-water shelf floored by continental crust. Some ferruginous chert beds contain greenalite nanoparticles, syneresis structures and shrinkage structures indicting a depositional origin from hydrothermal vent plumes.||Hamersley Group|West Angela Member, Paraburdoo Member, Bee Gorge Member.|Overlies the Marra Mamba Iron Formation, underlies the Mount Sylvia Formation.|Fine-grained siliciclastic and carbonate beds in upper parts intercalated with regional chert bands, includes laminated chert. Comprises shale, carbonate, minor Fe-chert and banded iron formation.|
20327|Wittenoom Formation|73290|5|Briefly described|p783, 785, 797||||||West Angela Member.|Overlies Marra Mamba Iron Formation|Carbonate-rich rocks.|
20327|Wittenoom Formation|73538|6|Mentioned|p4-5|||||Hamersley Group|Bee Gorge Member, Paraburdoo Member, West Angela Member|Underlain by the Mount Newman member of the Marra Mamba Iron Formation. Overlain by the Mount Sylvia Formation.|Includes mudstone/siltstone and carbonates.|
20327|Wittenoom Formation|73574|5|Briefly described|p763-764, p770|Proterozoic|Late Archean|||Hamersley Group|||Dolomitic.|
20341|Wodgina Hills quartzite|37539|6|Mentioned|Fig.1|||||||||
20348|Wogatti Sandstone|23815|4|Described|p293, 294|Neocomian|Tithonian|Geological Province: Carnarvon Basin. Overlying unit: Birdrong Sandstone (disconformable). Underlying unit: Learmonth Formation (conformable). Max. thickness: 107 m.||||||
20348|Wogatti Sandstone|24059|5|Briefly described|p138|Neocomian|Neocomian|Geological Province: Exmouth Sub-basin.  Maximum thickness: 107m.||||||
20348|Wogatti Sandstone|24160|5|Briefly described|p36|Cretaceous|Cretaceous|||Winning Group||Underlies part of Birdrong Sandstone.||
20348|Wogatti Sandstone|31561|5|Briefly described|p34|||Early Cretaceous||||||
20348|Wogatti Sandstone|32648|6|Mentioned|p32|||Jurassic||||||
20348|Wogatti Sandstone|33166|6|Mentioned|Table 1|||Correlation chart||||||
20348|Wogatti Sandstone|33386|6|Mentioned|Fig.7|||||||||
20348|Wogatti Sandstone|33453|4|Described|p71|||||||||
20348|Wogatti Sandstone|34363|6|Mentioned|p56|||Tithonian. See also Fig.7.||||||
20348|Wogatti Sandstone|34838|6|Mentioned|Fig.3|||||||||
20348|Wogatti Sandstone|35105|6|Mentioned|Fig.5|||||||||
20348|Wogatti Sandstone|36257|6|Mentioned|Table 2.1|||||||||
20348|Wogatti Sandstone|36890|3|Fully described|p293|||||||||
20348|Wogatti Sandstone|39427|4|Described|Table 1|||||||||
20348|Wogatti Sandstone|40617|6|Mentioned|p18|||||||||
20348|Wogatti Sandstone|41271|3|Fully described|p141|||||||||
20348|Wogatti Sandstone|41438|6|Mentioned|p108|||||||||
20348|Wogatti Sandstone|41440|4|Described|p137|||||||||
20348|Wogatti Sandstone|41446|6|Mentioned|p213|||||||||
20348|Wogatti Sandstone|42116|5|Briefly described|Fig.1 P6|||||||||
20348|Wogatti Sandstone|42615|6|Mentioned|p17|||||||||
20348|Wogatti Sandstone|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||01-JUN-06
20348|Wogatti Sandstone|60384|5|Briefly described|p243 Fig 2b|Early Cretaceous|Late Jurassic|Northern Carnarvon Basin.||||||
20348|Wogatti Sandstone|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Late Jurassic|||||||
20348|Wogatti Sandstone|67200|6|Mentioned|p17 table 1, p54|||Thermal conductivity of 2.83 W/mK||||||
20348|Wogatti Sandstone|69182|6|Mentioned|Ch3 p23-p27, Ch3 p69-p71|||||||||
20348|Wogatti Sandstone|69558|6|Mentioned|p258 fig 419|Early Cretaceous|Early Cretaceous|||||Unconformably overlies the Lyons Group. Overlies and is faulted against the Learmonth Formation. Overlain by the Birdrong Sandstone.||25-MAY-21
20388|Wombarella Quartz Gabbro|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20388|Wombarella Quartz Gabbro|30533|4|Described|p12|||On Table 1||||||
20388|Wombarella Quartz Gabbro|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20388|Wombarella Quartz Gabbro|32660|5|Briefly described|Table 1|||||||||
20388|Wombarella Quartz Gabbro|32728|5|Briefly described|p22|||See also Fig.3||||||
20388|Wombarella Quartz Gabbro|36551|6|Mentioned|Table 14|||||||||
20388|Wombarella Quartz Gabbro|36885|5|Briefly described|p167|||||||||
20388|Wombarella Quartz Gabbro|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
20388|Wombarella Quartz Gabbro|41594|5|Briefly described|p72|||||||||
20388|Wombarella Quartz Gabbro|41987|6|Mentioned|p70|||||||||
20388|Wombarella Quartz Gabbro|42710|5|Briefly described|map legend|Proterozoic||||||||
20388|Wombarella Quartz Gabbro|42811|5|Briefly described|p12|||||||||
20388|Wombarella Quartz Gabbro|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
20388|Wombarella Quartz Gabbro|44155|4|Described|p234 Tb.3-2, p239, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|See also p254 Fig.3-40. West Kimberley. Stratigraphic position uncertain. Intrudes metamorphics in Hooper Complex.||Hooper Complex.||Intruded by Lennard Granite, Kongorow Granite.|Orthopyroxene- and biotite-bearing quartz gabbro, microtonalite porphyry, and their metamorphic equivalents.|
20388|Wombarella Quartz Gabbro|45087|6|Mentioned|p73|||Chemical analyses||||||
20388|Wombarella Quartz Gabbro|50437|6|Mentioned|p2.1|||||||||
20388|Wombarella Quartz Gabbro|64580|6|Mentioned|map legend|||Of Paperbark Supersuite.||||||15-DEC-08
20388|Wombarella Quartz Gabbro|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Medium to fine grained biotite-pyroxene gabbro, quartz gabbro and quartz norite with some recrystallisation in places|
20388|Wombarella Quartz Gabbro|72437|5|Briefly described|p59|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Quartz diorite.|
20428|Wondoan Hill Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|24122|3|Fully described|p8, p5 Tb.1|Proterozoic|Proterozoic|Of Tijunna Group. Conformably overlain by Stubb Formation.  Max. thickness: 108m.  Geological Province: Victoria Basin.||||||19-DEC-06
20428|Wondoan Hill Formation|24297|3|Fully described|p14|Mesoproterozoic|Mesoproterozoic|Of Tijunna Group. Conformably overlain by Stubb Formation, unconformably overlies Bullita Group. Parts of this unit are now mapped as Jasper Gorge Sandstone. Maximum thickness: 145m.  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||19-DEC-06
20428|Wondoan Hill Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Glauconitic quartz sandstone, claystone, siltstone, mudstone.||||||19-DEC-06
20428|Wondoan Hill Formation|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group.   Geological Province: Victoria Basin.||||||19-OCT-12
20428|Wondoan Hill Formation|24441|5|Briefly described|p1 Fig. 1,  Appendix 2-1:2|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Upper part is sandstone; lower is siltstone and mudstone. Unconformably overlies the Banyan Formation and Battle Creek Formation; overlain by Stubb Formation. Thickness: 111m. Geological Province: Victoria Basin.||||||08-AUG-05
20428|Wondoan Hill Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Tijunna Group.  Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|28255|3|Fully described|p58, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Lower glauconitic sst-sltst sequence, middle claystone and upper sst. Unconformable on Bynoe Fm, Weaner Sst and Battle Creek Fm; on WAVE HILL sheet it  is unconf. on Nero Sltst and Mount Gordon Sst. Unconformable below Stubb Fm and Jasper Gorge Sst. 145m.||||||15-JUN-05
20428|Wondoan Hill Formation|30003|4|Described|p7, p13|||Of the Bullita Group.  White and purple blocky to flaggy medium-bedded fine quartz sandstone; grey to purple flaggy to fissile thin-bedded to laminated fine siltstone, glauconitic in part. Max. thickness: 120m. Carpentarian or Adelaidean.||||||19-DEC-06
20428|Wondoan Hill Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
20428|Wondoan Hill Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Glauconitic quartz sandstone, white claystone and siltstone, brown mudstone.||||||02-DEC-04
20428|Wondoan Hill Formation|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|32660|5|Briefly described|Table 6|||||||||
20428|Wondoan Hill Formation|32728|6|Mentioned|p16|||||||||
20428|Wondoan Hill Formation|32775|5|Briefly described|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||02-DEC-04
20428|Wondoan Hill Formation|33373|3|Fully described|p9|||On Table 2.||||||
20428|Wondoan Hill Formation|33374|6|Mentioned|p8|||See also p12. Strat. table.||||||19-DEC-06
20428|Wondoan Hill Formation|33375|6|Mentioned|p8 Tb. 1, p12|Adelaidean|Adelaidean|Laminated green siltstone and shale; interbeds of glauconitic sandstone.  Unconformably overlies Bynoe Formation (Bullita Group); unconformably overlain by Jasper Gorge Sandstone.||||||27-APR-05
20428|Wondoan Hill Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|33377|5|Briefly described|Table 2|||Stratigraphy.||||||
20428|Wondoan Hill Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Green siltstone and shale; interbeds of glauconitic sandstone.||||||27-APR-05
20428|Wondoan Hill Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20428|Wondoan Hill Formation|37462|4|Described|Table 4.VI|||||||||
20428|Wondoan Hill Formation|38157|6|Mentioned|p284|||||||||
20428|Wondoan Hill Formation|45112|3|Fully described|p29|||See also p30.||||||19-DEC-06
20428|Wondoan Hill Formation|45140|6|Mentioned|p13|||Victoria River region.||||||
20428|Wondoan Hill Formation|48942|2|Defined|p57|Adelaidean|Adelaidean|Strat. section p113. Prob. Adelaidean.||||||19-DEC-06
20428|Wondoan Hill Formation|48943|3|Fully described|p69|||||||||
20428|Wondoan Hill Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fine quartz sandstone, siltstone. Of Tijunna Group. Geological Province: Victoria Basin.||||||11-JAN-05
20428|Wondoan Hill Formation|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Tijunna Group. Unconformable on Bullita Group; conformable below Stubb Formation; also unconformable below Jasper Gorge Formation. Max. thickness: 145m. Geological Province: Victoria Basin.||||||
20428|Wondoan Hill Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Tijunna Group.||Unconformably overlies uppermost units of Bullita Group. Is overlain by Stubb Formation.||
20428|Wondoan Hill Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Tijunna Group.||Unconformably overlies Bynoe Formation. Is overlain by Jasper Gorge Sandstone.|Siltstone and shale; interbeds of glauconitic sandstone.|
20428|Wondoan Hill Formation|68733|5|Briefly described|p177 Fig.2, p179, p183-186, p191-192|||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). Sm-Nd isotope data tabulated.||Of the Tijunna Group.||Conformably overlain by the Stubb Formation.||06-DEC-17
20428|Wondoan Hill Formation|69432|4|Described|p17:2, 12-13, 15|||Birrindudu Basin. Thins from >140m in the N to <30m in the S. Considerable lateral variation in composition. Where the unit is thin, it is almost all sandstone, with subordinate shale and siltstone only in the lower part. Uplift was probably active prior to or during deposition of this unit. Thick shale may possibly have some potential as petroleum source rock.||Tijunna Group.||Unconformably overlies Banyan Formation (Bullita Group).|Basal cross-bedded sandstone, overlain by a succession of more thinly-bedded sandstone (commonly glauconitic), siltstone, mudstone and black shale. Upper parts contain diagenetic nodules, rare hematite, disseminated pyrite and galena.|12-JUL-16
20428|Wondoan Hill Formation|69673|6|Mentioned|p48 fig 35, p51|||||Tijunna Group||Unconformably overlies Banyan Formation, Battle Creek Formation, overlain by Stubb Formation||
20428|Wondoan Hill Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Tijunna Group.||Unconformably overlies Bynoe Formation. Is ?unconformably overlain by Jasper Gorge Sandstone.|Siltstone and shale; interbeds of glauconitic sandstone.|21-JAN-22
20428|Wondoan Hill Formation|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Bynoe Formation (Bullita Group). Is overlain conformably by Stubb Formation.|Glauconitic quartz sandstone, claystone, siltstone, mudstone.|
20428|Wondoan Hill Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Mount Gordon Sandstone (Bullita Group). Unconformably overlain by the Jasper Gorge Sandstone.|Fine quartz sandstone, siltstone.|21-SEP-17
20428|Wondoan Hill Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tijunna Group.||Unconformably overlies Battle Creek Formation. Is overlain by Stubb Formation.|Glauconitic quartz sandstone, claystone, siltstone, mudstone.|
20428|Wondoan Hill Formation|70968|2|Defined|p115-120, p124, p126-127, p129, p131-132|Mesoproterozoic|Mesoproterozoic|See also p138. Originally included in the former Victoria River Group by Traves (1955), and in the former Coolibah Formation by Laing and Allen (1956). Although recognised as occurring between Bynoe and Stubb Formations, was unassigned  by Sweet et al. (1974). Named after Wondoan Hill near Fitzroy homestead, but the exposures there were subsequently remapped as Jasper Gorge Sandstone. The type locality is at the E end of Fitzroy Range; the section measured by Sweet et al. (1974), 9km due S of Wondoan Hill, is now inaccessible and a new type locality is needed. Lithology well described and very well illustrated. 30-145m thick. Shallow-marine inner shelf to shoreface deposits. Various age determination attempts described. Detrital zircon diagram.|c.1575 Ma (maximum depositional age).|||Unconformably overlies Battle Creek, Bynoe Formations; Weaner, Mount Gordon Sandstones; Nero Siltstone. Is overlain by Stubb Formation conformably, and Jasper Gorge Sandstone unconformably.|Glauconitic and quartz sandstone, glauconitic siltstone, claystone and minor dolomitic siltstone. Shows considerable lateral variation in composition.|
20428|Wondoan Hill Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone, claystone|
20428|Wondoan Hill Formation|71302|5|Briefly described|p6,72,74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: c. 1575 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Contain small c > 1560-1640 Ma age populations.||Unit of Tijunna Group.||Overlain by Stubb Formation. Underlain by Banyan Formation and Battle Creek Formation.||
20428|Wondoan Hill Formation|71893|4|Described|iii, p2-p3, p7-p8, p68-p71|||Birrindudu Basin. A maximum depositional age of 1575 +/- 16 Ma was derived and isolated younger ages to ca 1452 Ma were also found. A shallow marine shelf to shoreface environment is interpreted. Sedimentary structures provide evidence for energetic shallow marine conditions. Description, sampling location, zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Tijunna Group||Unconformably overlies the Bullita Group. Conformably overlain by the Stubb Formation.|Interbedded glauyconitic and quartz sandstone, siltstone and claystone.|
20428|Wondoan Hill Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Tijunna Group||Overlain by Stubb Formation.||
20428|Wondoan Hill Formation|73083|6|Mentioned|p45-46|Mesoproterozoic|Mesoproterozoic|Victoria Basin. Weak magnetic response.|||||Siliciclastic.|
20450|Wongida Creek Granodiorite|42435|6|Mentioned|Fig.1 P43|||? Related to Wongida Dolomite Member?||||||
20450|Wongida Creek Granodiorite|72758|5|Briefly described|p4 Fig.1, p9-10 Tb.1, p45-46.|||Shown as Wongida Granodiorite on Wyloo Structural Sketch Map p4 Fig.1. Probable igneous source rocks, crustal origin. Named by Daniels (1965).||||Intrudes Ashburton Formation, Morrisey Metamorphic Suite.|Mainly medium- to coarse-grained biotite granodiorite. Includes a muscovite-rich tourmaline granite facies near western margin. Contains mafic xenoliths, large xenoliths of tourmalinized schist.|
20481|Woodbine Group|13354|6|Mentioned|p375 Fig.6.|Tertiary|Late Cretaceous|Comprises Bassett, Grebe, Prion, Cartier, Oliver and Barracouta Formations. Overlies Bathurst Island Group.||107||||28-OCT-14
20481|Woodbine Group|23378|4|Described|p180 Fig.2|Quaternary|Tertiary|of Vulcan Sub-basin.||||||01-MAR-10
20481|Woodbine Group|42056|4|Described|p100|||||||||
20481|Woodbine Group|42066|5|Briefly described|Fig.3 P199|||||||||
20481|Woodbine Group|60634|6|Mentioned|p1168 Fig.3. |Cenozoic|Cenozoic||||Includes Johnson, Grebe, Hibernia, Prion, Oliver and Barracouta Formations.|Overlies Bathurst Island Group.||
20481|Woodbine Group|61550|6|Mentioned|p495 Fig.2. |Cenozoic|Cenozoic||||Includes the Barracouta, Oliver, Prion, Hibernia, Grebe and Johnson Formations.|Overlies Bathurst Island Group.||
20481|Woodbine Group|62508|5|Briefly described|p31|Tertiary|Tertiary|||||||
20481|Woodbine Group|62510|5|Briefly described|p4|Cenozoic|Cenozoic|Geological Province: Money Shoal Basin.||||||
20481|Woodbine Group|63062|4|Described|p9 Fig. 9, p36, p33 Fig. 30|Pleistocene|Miocene|Thickness: <400m in study area, ~800m at Tuatara. Geol.Prov: Arafura/Money Shoal Basins. Coarse, quartzitic sandstones with claystone interbeds, and minor coal and dolomite overlain by calcareous claystone and marl with calcarenite interbeds.||||||07-FEB-11
20481|Woodbine Group|66187|5|Briefly described|p413 Fig.2|Eocene|Oligocene|Mount Ashmore Dome. Includes Oliver, Prion, Hibernia, Grebe and Johnson Formations.||||||
20481|Woodbine Group|69297|6|Mentioned|p283,  p285, p305, p322|Upper Neogene|Upper Neogene|Money Shoal Basin.|||Includes the Bassett Formation, Cartier Formation, Oliver Formation and the Barracouta Shoal Formation.|Unconformably overlies the Bathurst Island Group.|Shallow marine carbonates.|
20481|Woodbine Group|69451|6|Mentioned|p35:3 Fig.35.4;|Cenozoic|Cenozoic|||||||12-JUL-16
20481|Woodbine Group|69452|4|Described|p36:4-5, 8, 15, 22|Holocene|Paleocene|McLennan et al. (1990). Petrel Sub-basin, Bonaparte Basin. Offshore; up to 1300m thick. A depositional hiatus occurred during the Miocene. Marine shelf deposits. The individual Formations have not been differentiated in the SE Bonaparte Basin.|||Johnson, Hibernia, Prion, Cartier, Oliver, Barracouta Shoal, Formations.|Unconformably overlies Bathurst Island Group.|A lower, sandy succession grading upwards into widespread shelf carbonate rocks.|12-JUL-16
20481|Woodbine Group|69456|4|Described|p40:1-2, 4, 6, 8-9, 15 Fig.40.16|Holocene|Miocene|McLennan et al. (1990). Bonaparte Basin. Rocks in the Money Shoal Basin are consistently referred to as "Woodbine Group equivalent" (to the Bonaparte Basin succession). Not yet recognised in onshore areas. Shallow-marine to deltaic depositional environment; alternating fluvial and shallow-marine at top. Generally <400m thick, thickening to the W to >1300m in Lynedoch-1. In the Bonaparte Basin, this Group contains Paleogene units of equivalent age to the Van Diemen Sandstone. Generally undeformed.||||Unconformably overlies offshore Bathurst Island Group and ?Van Diemen Sandstone.|Lower unit of coarse quartzite sandstone with claystone interbeds, minor coal and dolostone; upper unit of calcareous claystone and marl with calcarenite interbeds (drillhole Cobra-1A).|12-JUL-16
20481|Woodbine Group|69458|6|Mentioned|p42:6, 18|Neogene|Paleogene|Bonaparte Basin.||||||12-JUL-16
20481|Woodbine Group|69653|6|Mentioned|p8, 10|Oligocene|Paleocene|Petrel Sub-basin.||||Overlies Wangarlu Formation (Bathurst Island Group).||
20481|Woodbine Group|69673|6|Mentioned|p166 fig 136, p174||||||Includes Johnson Formation, Hibernia Formation, Prion Formation, Oliver Formation, Barracouta Shoal Formation|||
20481|Woodbine Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Holocene|Danian|See also Regional geology: Figs.6-7. Sahul: Fig.2, p3. Vulcan: Fig.2, p3. Carbonates form an intraformational seal in Sahul Syncline and Vulcan Sub-basin.|||Johnson, Hibernia, Prion, Oliver and Barracouta Shoal Formations.|Overlies Bathurst Island Group.||12-JUL-16
20481|Woodbine Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Holocene|Paleocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Johnson, Bassett, Cartier, Oliver and Barracouta Shoal Formations.|Overlies Bathurst Island Group.||12-JUL-16
20481|Woodbine Group|70098|5|Briefly described|p18 Fig.4, p19 Fig.5|Cenozoic|Cenozoic|Money Shoal Basin.||||Overlies Bathurst Island Group.||
20494|Wooden Duck Member|23404|5|Briefly described|p645|||Of Mainoru Formation.||||||
20494|Wooden Duck Member|23937|2|Defined|p96  App. 1|Calymmian|Calymmian|Of the Mainoru Formation. Conformably overlain by Showell Member; conformably overlies the Mountain Valley Limestone Member. Age: >1493+/-4 Ma. Max. thickness: >350m.  Geological Province: McArthur Basin.||||||18-APR-05
20494|Wooden Duck Member|24050|4|Described|p44, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Laminated mudstone; laminated siltstone and micaceous galuconitic sandstone; minor limestone.  Of the Mainoru Formation.  Max. thickness: ?70m.||||||20-DEC-06
20494|Wooden Duck Member|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mainoru Formation (Roper Group). Geological Province: McArthur Basin.||||||20-DEC-06
20494|Wooden Duck Member|40691|6|Mentioned|Fig.4|||||||||
20494|Wooden Duck Member|41268|5|Briefly described|Fig.4|||||||||
20494|Wooden Duck Member|44434|14|Not recorded|p.7, opp. p.6, map|||Member of Mainoru Formation (Roper Group).||||||
20494|Wooden Duck Member|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
20494|Wooden Duck Member|44471|14|Not recorded|p.9, opp.p.7, map|||(D53-10).||||||
20494|Wooden Duck Member|44472|5|Briefly described|map legend|||Of the Mainoru Formation.  Flaggy quartz greywacke, micaceous greywacke, few galuconitic bands.  Upper (?) Proterozoic.||||||02-DEC-04
20494|Wooden Duck Member|45162|6|Mentioned|Fig.4|||||||||
20494|Wooden Duck Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group).  Dark green to grey laminated mudstone; with thinly bedded siltstone and fine-grained sandstone; thin to thick bedded micaceous and glauconitic fine-grained sandstone; minor laminated limestone.||||||22-FEB-05
20494|Wooden Duck Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Dark grey to green laminated mudstone with thinly interbedded siltstone and fine grained sandstone; thin to thick bedded micaceous and glauconitic fine grained sandstone.||||||
20494|Wooden Duck Member|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Mainoru Formation.||||
20494|Wooden Duck Member|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 55m to over 350m thick. Storm-dominated shelf deposits.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Greyish-green mudstone and fine micaceous glauconitic sandstone.|12-JUL-16
20494|Wooden Duck Member|70734|5|Briefly described|p14, 16|||McArthur Basin. Age consistent with Re-Os age of Velkerri Formation, higher in succession. Storm-dominated shelf (mudstone-dominated), top sandstone-dominated.|SHRIMP age 1492+/-4 Ma from tuff.|Of Mainoru Formation.||||
20494|Wooden Duck Member|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic||1492 +/- 4 Ma (U-Pb zircon).|Mainoru Formation||Overlies Mountain Valley Limestone Member; overlain by Showell Creek Member.|Interbedded mudstone, siltstone and fine sandstone.|
20494|Wooden Duck Member|70968|2|Defined|p17-18,p20,p30-33,p130-131,p140,p143-144|Calymmian|Calymmian|Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Named after Wooden Duck Creek. The type section is from 373800mE 8437400mN (base) to 374000mE 8437300mN in NW URAPUNGA sheet. Very similar mineralogy and texture to Showell Member: difficult to tell apart. Forms prominent escarpments with sandstone caps. Lithology described and illustrated. Thickness from 17m to 130m. Shallowing-upward marine-shelf sucession.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Dominantly mudstone interbedded with very fine- to rarely medium-grained, commonly micaceous and glauconitic sandstone that increases in frequency up-section. Rare limestone or dolostone in middle part.|
20494|Wooden Duck Member|71059|4|Described|p3, p20|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 56-130m thick. Storm-dominated marine shelf deposits. Organic petrology reflectivity data tabulated.||Mainoru Formation.||Conformably overlies Mountain Valley Limestone Member. Is overlain conformably by Showell Member.|Grey-green mudrocks interbedded with usually very fine micaceous glauconitic sandstone, rare limestone.|
20494|Wooden Duck Member|71488|5|Briefly described|p141 fig 1b|Calymmian|Calymmian||1492 +/- 4 Ma|Mainoru Formation||Overlies the Mountain Valley Limestone Member. Overlain by the Showell Creek Member.||
20494|Wooden Duck Member|71494|4|Described|p2-p4, p6-p13, p15, p17-p19, p26|||Thickness ranges from 55 to 350 metres plus. Deposited in a storm-dominated shelf environment. Identified as the Wood sequence by Abbott and Sweet (2000) in their sequence stratigraphic interpretation of the Roper Group. Core log features presented in this volume.||Mainoru Formation||Conformably overlies the Mountain Valley Limestone Member. Conformably overlain by the Showell Member.|Greyish-green mudstone and fine micaceous glauconitic sandstone.|
20494|Wooden Duck Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Mainoru Formation||||24-SEP-18
20494|Wooden Duck Member|73242|5|Briefly described|p39|Calymmian|Calymmian|Geochron are U-Pb zircon ages [see Fig. 2].|1492 +/- 4 Ma, 1493 +/- 4 Ma|Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Mountain Valley Limestone Member. Overlain by Showell Member.|Includes interbedded mudstone and fine sandstone with marine shelf sandstone.|
20509|Woodlands Arenite Member|23723|4|Described|p21|Proterozoic|Proterozoic|Of Gap Well Formation. Geological Province: Jillawarra basin. Max. thickness: 250 m.||||||01-FEB-12
20509|Woodlands Arenite Member|23724|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Gap Well Formation.||||||
20509|Woodlands Arenite Member|23725|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Gap Well Formation.||||||
20509|Woodlands Arenite Member|41144|5|Briefly described|Table 2|||||||||
20522|Woodleigh Formation|12729|4|Described|p.15, 25-6, 28, 32, 34; Fig. 4.|Early Jurassic|Early Jurassic|Type section: Woodleigh 7 waterbore (210-235 m). Max thickness of 126 m (Carpentaria CB 4). Restricted to the Woodleigh impact structure (as lacustrine silt and mud deposit). Age from abundant spores and pollens (McWhae et al., 1958). Assigned to the Callialasporites turbatus Zone (Toarcian-Bajocian).|||||Weakly indurated, non-marine, shaly succession.|
20522|Woodleigh Formation|12731|6|Mentioned|p592.|Late Jurassic|Late Jurassic|Thin locally-restricted lacustrine deposits found over a circular gravity anomaly, possibly a pre-Early Jurassic impact structure on Woodleigh Station.||||||
20522|Woodleigh Formation|14228|5|Briefly described|p5 fig 2, p9|Early Jurassic|Early Jurassic|Restricted to the central 50 km of the Woodleigh impact structure. Apatite fission-track analyses of the Formation imply an original thickness of about 1100 m, before uplift and erosion, associated with breakup, removed about 700 m.|||||Interbedded shale and sandstone unit of lacustrine origin.|06-OCT-16
20522|Woodleigh Formation|23572|4|Described|p3|Early Jurassic|Early Jurassic|Geological Province: Carnarvon Basin. Max. thickness: 298m.||||||
20522|Woodleigh Formation|23935|4|Described|p11 Fig.7|Hettangian|Hettangian|Unconformably overlain by Winning Group. Laminated siltstone and mudstone interbedded with fine-grained silty sandstone. Deposited in a deep, anoxic lacustrine environment. Max. thickness: 298 m. Geological Province: Southern Carnarvon Basin.||||||
20522|Woodleigh Formation|24351|5|Briefly described|Plate 4 (in pocket)|Early Jurassic|Early Jurassic|Geological Province: Gascoyne Platform/Sub-basin.||||||13-DEC-07
20522|Woodleigh Formation|40617|6|Mentioned|p18|||||||||
20522|Woodleigh Formation|41271|3|Fully described|p132|||||||||
20522|Woodleigh Formation|49942|5|Briefly described|p4 Fig.3, p38|Early Jurassic|Early Jurassic|Lacustrine. Geological Province: Gascoyne Platform.||||||
20522|Woodleigh Formation|60384|6|Mentioned|p243 Fig 2a|Early Jurassic|Late Triassic|Southern Carnarvon Basin.||||||
20522|Woodleigh Formation|60725|6|Mentioned|p33 Fig.4.|Early Jurassic|Early Jurassic|||||||
20522|Woodleigh Formation|61560|6|Mentioned|p493|Jurassic|Jurassic|Lacustrine deposits.||||||
20522|Woodleigh Formation|61562|5|Briefly described|p546-547|Early Jurassic|Early Jurassic|Lacustrine deposits.||||||15-DEC-05
20522|Woodleigh Formation|61563|5|Briefly described|p576|Early Jurassic|Early Jurassic|Lacustrine deposits. Overlies the centre part of the Woodleigh impact structure.  See also p579 Fig. 3.||||||15-DEC-05
20522|Woodleigh Formation|61564|5|Briefly described|p596-7|Early Jurassic|Early Permian|||||||
20522|Woodleigh Formation|67200|6|Mentioned|p17 table 1, p54|||Thermal conductivity of 1.63 W/mK||||||
20522|Woodleigh Formation|69182|6|Mentioned|Ch3 p12-p13|||Perth Basin.||||||
20522|Woodleigh Formation|69297|6|Mentioned|p249|Pleinsbachian|Hettangian|Gascoyne Sub-basin of the Southern Carnarvon Basin.||||Unconformably overlies the Lyons Group. Unconformably overlain by the Birdrong Sandstone or the Muderong Shale.||
20522|Woodleigh Formation|69583|5|Briefly described|p141|Early Jurassic|Early Jurassic|Up to 300m thick.|||||Siliciclastic lacustrine deposits.|
20545|Woolaga Limestone Member|15881|5|Briefly described|p62 Fig. 1|Permian|Permian|Of Holmwood Shale in Woolaga Creek area. Contains ammonoids.||||||12-FEB-09
20545|Woolaga Limestone Member|23172|4|Described|Map Legend|Permian|Permian|||||||
20545|Woolaga Limestone Member|23174|6|Mentioned|p10|||||||||
20545|Woolaga Limestone Member|23279|6|Mentioned|p12|||||||||
20545|Woolaga Limestone Member|23816|4|Described|p232|Sakmarian|Sakmarian|Geological Province: Perth Basin. Of the Holmwood Shale. Max. thickness: 1 m. Fossiliferous.||||||27-APR-05
20545|Woolaga Limestone Member|36293|6|Mentioned|p91|||||||||
20545|Woolaga Limestone Member|36890|4|Described|p232|||||||||
20545|Woolaga Limestone Member|41514|5|Briefly described|p62|||Of the Holmwood Shale.  Contains ammonoids.||||||18-AUG-08
20545|Woolaga Limestone Member|44144|6|Mentioned|p508 Tb. 4-21|Sakmarian|Sakmarian|||Holmwood Shale|||Fossiliferous limestone.|
20545|Woolaga Limestone Member|61811|5|Briefly described|p36.|Permian|Permian|Lenticular calcareous facies of restricted areal extent.||Unit in Holmwood Shale.||||
20545|Woolaga Limestone Member|64635|6|Mentioned|p18-19 |Sakmarian|Sakmarian|||Unit in Holmwood Shale.|||Local, lenticular calcareous facies.|
20545|Woolaga Limestone Member|64974|6|Mentioned|p144 Fig. 3|Sakmarian|Sakmarian|Geological Province: Perth Basin.||||||24-JUN-09
20545|Woolaga Limestone Member|73623|5|Briefly described|p3-4, 6|||Playford (1959). Irwin Basin.||Holmwood Shale||Equivalent to Woolaga Limestone Member.|Localised nodular limestone deposits containing unusual fossil biota including tube worms, bivalve-like shells, gastropods and ammonoids.|
20549|Woolaston Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228 Fig. 18|Late Cretaceous|Late Creatceous|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
20549|Woolaston Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||Overlies Jamieson Formation. Is overlain by Fenelon and Gibson Formations.||
20549|Woolaston Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||Overlies Jamieson Formation. Is overlain by Fenelon and Gibson Formations.||
20549|Woolaston Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Jamieson Formation and underlies Fenelon and Gibson Formations.||103||||28-OCT-14
20549|Woolaston Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Cretaceous|Of the Bathurst Island Group.||||||01-MAR-10
20549|Woolaston Formation|23378|4|Described|p180 Fig.2, p182||Late Cretaceous|Of the Bathurst Island Group. In the Vulcan Sub-basin.||||||01-MAR-10
20549|Woolaston Formation|24171|6|Mentioned|p729|||See also the misspelt Woollaston Formation.||||||20-DEC-06
20549|Woolaston Formation|24207|5|Briefly described|p209 Fig.5, p218|Cenomanian|Cenomanian|Geological Province: Vulcan Sub-basin.||||||01-MAR-10
20549|Woolaston Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
20549|Woolaston Formation|42053|5|Briefly described|Fig.2 p29|||||||||20-SEP-17
20549|Woolaston Formation|42066|5|Briefly described|Fig.3 P199|||||||||
20549|Woolaston Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
20549|Woolaston Formation|60385|6|Mentioned|p270, p272 Fig 3, p276|Campanian|Cenomanian|Browse Basin.|||||Pelagic marl, hemipelagic marl, limestone.|
20549|Woolaston Formation|60634|6|Mentioned|p1168 Fig.3. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson Formation. Is overlain by Gibson Formation.||
20549|Woolaston Formation|61548|6|Mentioned|p480 Fig.3|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||||
20549|Woolaston Formation|61550|6|Mentioned|p495 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Jamieson Formation. Is overlain by Gibson Formation.||
20549|Woolaston Formation|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Age: ~95-~86Ma. Geological Province: Vulcan Sub-basin, Londonderry High and Northern Bonaparte Basin.||||||01-MAR-10
20549|Woolaston Formation|63358|5|Briefly described|p4 Fig. 1.3|Santonian|Cenomanian|See also p133 Fig. 3.71.||||||01-MAR-10
20549|Woolaston Formation|64695|5|Briefly described|p262 Fig.8|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Is overlain by Gibson Formation.||
20549|Woolaston Formation|64697|5|Briefly described|p84 Fig.2 |Late Cretaceous|Late Cretaceous|||||||
20549|Woolaston Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Campanian|Turonian|Bathurst Island Group. Underlies the Gibson Formation, overlies the Jamieson Formation. Mount Ashmore Dome. Deep water limestone.||||||
20549|Woolaston Formation|68223|6|Mentioned|p178 Fig.3|Coniacian|Cenomanian|||||||
20549|Woolaston Formation|69297|6|Mentioned|p305|Coniacian|Cenomanian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. See also reference to lower Woolaston Formation p303.||Bathurst Island Group||Overlies the Upper Jamieson Formation. Overlain by the Gibson Formation.|Siltstone and shale.|20-SEP-17
20549|Woolaston Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
20549|Woolaston Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Turonian|Cenomanian|See also Sahul: Fig.2, p1-2. Vulcan: Fig.2. Reservoir carbonates in Sahul Syncline.||Bathurst Island Group.||Overlies Jamieson and Wangarlu Formations. Is overlain by Brown Gannet Limestone.||12-JUL-16
20549|Woolaston Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Turonian|Cenomanian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin. Not present in Yampi and Leveque Shelves.||Bathurst Island Group.||Overlies Upper Jamieson Formation. Is overlain by Brown Gannet Limestone.||12-JUL-16
20554|Woolgangie Monzogranite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Recrystallised monzogranite and granodiorite|
20554|Woolgangie Monzogranite|41914|4|Described|p19|||||||||
20554|Woolgangie Monzogranite|42698|5|Briefly described|map legend|||||||||
20554|Woolgangie Monzogranite|42892|4|Described|p41|||||||||
20554|Woolgangie Monzogranite|60076|5|Briefly described|p46 App. 1|||[Agmwo]   Recrystallised monzogranite and granodiorite.||||||
20554|Woolgangie Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Recrystallized monzogranite and granodiorite.||||||07-FEB-11
20554|Woolgangie Monzogranite|68066|5|Briefly described|p5 Fig. 2, p18, p22-24, map|Archean|Archean|Texturally distinct recrystallized granular granitoid compositionally indistinguishable from Burra Monzogranite. Intruded parallel to the margins of the Burra Monzogranite. Woolgangie Monzogranite is undeformed and all diagnostic dyke suites found in the Burra Monzogranite are cut by it.|||||Recrystallized monzogranite and granodiorite; typically coarse-grained, granoblastic, and lacks foliation; xenoliths described in some detail.|
20554|Woolgangie Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Recrystallized monzogranite and granodiorite.|07-AUG-15
20554|Woolgangie Monzogranite|69559|5|Briefly described|GA_geochron.csv||Neoarchean|The strong reverse discordance of some data probably results from extreme metamictisation of those grains. The most concordant analyses are also variable in age and, given the high U-contents, it is likely that many of the analyses represent minimum ages. Fletcher, I.R. McNaughton, N.J. 2001.|Min age: 2706+/-7 Ma U/Pb SHRIMP||||Felsic intrusive.|
20554|Woolgangie Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Monzogranite and granodiorite, recrystallised (metamorphosed).|
20554|Woolgangie Monzogranite|70794|6|Mentioned|GA_geochron.csv|Neoarchean|Neoarchean|Dating of sample 97969034 discussed. Interpreted as minimum age of emplacement, but it seems more likely that all most of these grains are xenocrysts in a rock with a magmatic age ~2630 Ma..|2706+/-7 Ma SHRIMP||||Felsic intrusive|
20554|Woolgangie 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.|3010-2600 Ma (inferred)||||Monzogranite and granodiorite; metamorphosed|
20591|Woolyeenyer Formation|22682|5|Briefly described|Fig9,p14||Archean|||||||07-NOV-08
20591|Woolyeenyer Formation|23136|6|Mentioned|p265 Fig.1|||||||||
20591|Woolyeenyer Formation|23159|5|Briefly described|p790 fig4 table5|Archean|Archean|||||||07-NOV-08
20591|Woolyeenyer Formation|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
20591|Woolyeenyer Formation|23926|5|Briefly described|p9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
20591|Woolyeenyer Formation|30562|2|Defined|p10|Archean|Archean|See also p37.||||||07-NOV-08
20591|Woolyeenyer Formation|31093|6|Mentioned|Fig. 4|||||||||
20591|Woolyeenyer Formation|36869|6|Mentioned|p48|||||||||
20591|Woolyeenyer Formation|41432|5|Briefly described|p13|||||||||
20591|Woolyeenyer Formation|42155|6|Mentioned|p369|||||||||
20591|Woolyeenyer Formation|42195|5|Briefly described|p143|||See also fig. 2.||||||
20591|Woolyeenyer Formation|42221|6|Mentioned|p33|||||||||
20591|Woolyeenyer Formation|42626|6|Mentioned|p8|||||||||
20591|Woolyeenyer Formation|42937|5|Briefly described|p559|||||||||
20591|Woolyeenyer Formation|43102|6|Mentioned|p11|||||||||
20591|Woolyeenyer Formation|43162|6|Mentioned|6,8|||U-Pb age: 2714+/-5 Ma||||||
20591|Woolyeenyer Formation|50542|6|Mentioned|p135|Archean|Archean|Consists of metabasalts. Geological Province: Yilgarn Craton.||||||07-FEB-11
20591|Woolyeenyer Formation|60076|5|Briefly described|p15, p16 Fig. 6|||A monotonous sequence of of massive basalt flows with a minor ultramafic component.  Overlies the Noganyer Formation; overlain by Mount Kirk Formation.  Max. thickness: 10m.  Geological Province: Gindalbie domain (Yilgarn Craton).||||||13-APR-05
20591|Woolyeenyer Formation|64633|6|Mentioned|p6 Fig.4.|||Kalgoorlie Terrane.||||Is overlain unconformably by Mount Kirk Formation.|Basalt, often pillowed; komatiite; dolerite/gabbro intrusions.|
20591|Woolyeenyer Formation|65264|5|Briefly described|p11|Archean|Archean|Min. age: 2714+/-5Ma (Hill et al 1992 - from a fractionated intrusion). Overlies Noganyer Formation. Geological province: Norseman terrane. Monotonous sequence of massive basalt flows with a minor ultramafic component.||||||07-FEB-11
20591|Woolyeenyer Formation|66880|5|Briefly described|pp7-8.|Archean|Archean|Norseman Terrane. This age is of a synvolcanic dolerite sill, correlated with Lunnon Basalt.|2714 +/- 5 Ma (Hill et al. 1992).|||Overlies Noganyer Formation. Is unconformably overlain by Mount Kirk Formation.|Basalt, often pillowed; komatiite; dolerite/gabbro intrusions.|
20591|Woolyeenyer Formation|70326|4|Described|p360,362,364-365|Neoarchean|Neoarchean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Woolyeenyer Basalt on p365]. Contains an intrusive basalt in the lower section with granophyric interval of mafic intrusion (2714+\-5 Ma; Hill et al., 1992),||||Overlain by Mount Kirk Formation. Underlain by Noganyer Formation.|Pillow lavas, minor mudstone and felsic rocks.|
20591|Woolyeenyer Formation|71166|6|Mentioned|p14|||||||||
20591|Woolyeenyer Formation|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Kambalda Sequence||||
20612|Woora Woora Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
20612|Woora Woora Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Disappointment Group, Officer Basin.||||||
20612|Woora Woora Formation|23590|5|Briefly described|p14|||Previously of the now-superseded Savory Group. Of Disappointment Group. Geological Province: Officer Basin.||||||
20612|Woora Woora Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
20612|Woora Woora Formation|23730|4|Described|p13|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Underlying unit Tchukardine Formation. Geological Province: Officer Basin.||||||
20612|Woora Woora Formation|23760|4|Described|p31|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Geological Province: Officer Basin.||||||
20612|Woora Woora Formation|42708|5|Briefly described|Plate 1|Proterozoic||Reserved as Woora Woora.||||||
20612|Woora Woora Formation|43756|6|Mentioned|Fig.2,p535|||||||||
20612|Woora Woora Formation|44111|6|Mentioned|p.58, Fig. 2|||in Savory Basin||||||
20612|Woora Woora Formation|62453|3|Fully described|p5 Fig. 3, 61|Ediacaran|Ediacaran|Of the Disappointment Group. Geological Province: Paterson Orogen. Overlies disconformably: Tchukardine Formation, Mundadjini Formation. Thickness: ~400m. Sandstone, siltstone, claystone.||||||27-JUN-06
20612|Woora Woora Formation|64580|4|Described|map legend||Neoproterozoic|Of Disappointment Group. Medium-grained ferruginous sandstone, lithic sandstone, quartz wacke, and siltstone.||||||09-DEC-08
20612|Woora Woora Formation|64772|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Disappointment Group but not represented in this study area.||||||07-FEB-11
20612|Woora Woora Formation|65410|6|Mentioned|p74.|||Savory Sub-basin. Its stratigraphic position is unclear: Supersequence 3 or 4.||||||
20612|Woora Woora Formation|65454|4|Described|p7 Fig.3, p11, p30 Fig.A1b|Paleozoic|Cambrian|Of Disappointment Group. Medium-grained ferruginous sandstone, lithic sandstone, quartz wacke and siltstone. Similar to McFadden Formation. Disconformably overlies Tchukardine Formation.||||||
20612|Woora Woora Formation|67202|5|Briefly described|p64|||NW Officer Basin.||Disappointment Group.||||
20612|Woora Woora Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Disappointment Group.||||
20612|Woora Woora Formation|69590|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|||Unit of Disappointment Group.|||Medium-grained ferruginous sandstone, lithic sandstone, quartz wacke, and siltstone|
20612|Woora Woora Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
20612|Woora Woora Formation|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Ediacaran|Officer Basin (Phase 1).||Disappointment Group|||Medium-grained ferruginous sandstone, lithic sandstone, quartz wacke, and siltstone.|
20639|Wotjulum Porphyry|23722|4|Described|p22|Proterozoic|Proterozoic|Intrudes the Kimberley Basin.||||||
20639|Wotjulum Porphyry|29946|6|Mentioned|Fig.1|||||||||
20639|Wotjulum Porphyry|30893|5|Briefly described|p205|||Lithology||||||
20639|Wotjulum Porphyry|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20639|Wotjulum Porphyry|30897|4|Described|p13|||||||||
20639|Wotjulum Porphyry|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20639|Wotjulum Porphyry|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20639|Wotjulum Porphyry|32660|5|Briefly described|Table 3|||||||||
20639|Wotjulum Porphyry|32728|6|Mentioned|Fig.3|||||||||
20639|Wotjulum Porphyry|36551|6|Mentioned|p27|||||||||
20639|Wotjulum Porphyry|36885|4|Described|p183|||||||||
20639|Wotjulum Porphyry|37228|6|Mentioned|Fig.2|||||||||
20639|Wotjulum Porphyry|37462|4|Described|Table4.III|||||||||
20639|Wotjulum Porphyry|42814|5|Briefly described|p15|||||||||
20639|Wotjulum Porphyry|42815|5|Briefly described|map|||||||||
20639|Wotjulum Porphyry|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Basin.||||||
20639|Wotjulum Porphyry|44140|5|Briefly described|p294, p299|Paleoproterozoic|Paleoproterozoic|Restricted to the Yampi area. Sills are up to 900m thick. Contemporaneous with the c.1762 Ma Hart Dolerite (although the 2 units never occur together).||||Intrudes upper Kimberley Group (Warton Sandstone, Elgee Siltstone, Pentecost Sandstone).|Grey-black quartz-feldspar porphyry.|08-MAR-18
20639|Wotjulum Porphyry|44155|6|Mentioned|p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|King Leopold Orogen, Kimberley region.||||||
20639|Wotjulum Porphyry|50009|6|Mentioned|p40|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20639|Wotjulum Porphyry|64580|4|Described|map legend||Paleoproterozoic|Quartz-feldspar porphyry.||||||09-DEC-08
20639|Wotjulum Porphyry|68078|4|Described|p7, p15, p19|Paleoproterozoic|Paleoproterozoic|Emplaced parallel to bedding in the Elgee Siltstone. A younger age is reported from previous unpublished work (McNaughton, 1999): 1725 +/- 12 Ma.|1740 Ma +/- 6 Ma(SHRIMP)|||Intrudes Elgee Siltstone|Porphyry with abundant phenocrysts of quartz, plagioclase and microcline in a fine grained groundmass of quartz, feldspar, biotite and sericite.Contact hornfels marked by the growth of andalusite and biotite porphyroblasts.|01-MAR-18
20639|Wotjulum Porphyry|69003|5|Briefly described|p5, p21|||Halls Creek Orogen. U-Pb zircon crystallisation age.|1725 Ma.|||Intrudes Warton Sandstone and Elgee Siltstone (Kimberley Group).||
20639|Wotjulum Porphyry|69585|6|Mentioned|p4-5, p27|Statherian|Statherian|Yampi Peninsula, western Lamboo Province.|1740 Ma.|||||
20639|Wotjulum Porphyry|69597|6|Mentioned|p5 fig 2b|||||||||
20639|Wotjulum Porphyry|69634|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological province: King Leopold Orogen. Generally intruded parallel to bedding, although some dykes are present. Contact hornfels with host rocks marked by growth of andalusite and biotite porphyroblasts. Previously dated at 1725+\-12 Ma (NJ McNaughton, 1999, written comm.; unpublished). See also geochron files.|1740+\-6 Ma (magmatic)|||Intrudes into Elgee Siltstone.|Quartz-feldspar porphyry|
20639|Wotjulum Porphyry|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1740 Ma||||Grey quartz--feldspar-phyric micromonzogranite|
20639|Wotjulum Porphyry|70731|6|Mentioned|p268|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
20639|Wotjulum Porphyry|70812|5|Briefly described|p6|Statherian|Statherian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1750 Ma|||||
20639|Wotjulum Porphyry|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
20639|Wotjulum Porphyry|70851|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province.|c. 1750 Ma|||||
20639|Wotjulum Porphyry|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: King Leopold Orogen. Events: North Australian Craton events (2500-250 Ma); Alice Springs Orogeny (450-295 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv and geochron files.|1740+\-6 to 1725+\-12 Ma (isotopic)|||Intrudes into Elgee Siltstone, Warton Sandstone, Pentecost Sandstone.|Grey quartz feldspar porphyry with phenocrysts of pink quartz and plagioclase and microcline|
20639|Wotjulum Porphyry|71281|5|Briefly described|p423|Paleoproterozoic|Paleoproterozoic|Age from zircons in sills.|1740 +/- 6 Ma (Wingate et al., 2011).|||Intrudes the Elgee Siltstone.||
20639|Wotjulum Porphyry|71397|5|Briefly described|p5-6|Statherian|Statherian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen.|c. 1740 Ma|||Intrudes into Kimberley Group.||28-NOV-19
20639|Wotjulum Porphyry|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|King Leopold Orogen.|Max age 1740+/-6 Ma, min 1725+/-12 Ma.||||Grey quartz--feldspar-phyric micromonzogranite.|
20639|Wotjulum Porphyry|72437|5|Briefly described|p12-13, p118|||Occurs on YAMPI where it intrudes the Elgee Siltstone (Tyler and Griffin, 1993). One whole rock analysis is provided.||||Intrudes the Elgee Siltstone.|Acid porphyry sill.|
20650|Wright Hill Formation|23818|6|Mentioned|p56|||||||||
20650|Wright Hill Formation|30807|6|Mentioned|p103|||Suggested map symbol||||||
20650|Wright Hill Formation|31457|6|Mentioned|p11|||||||||
20650|Wright Hill Formation|31965|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20650|Wright Hill Formation|34535|5|Briefly described|p56|||||||||
20650|Wright Hill Formation|41751|6|Mentioned|p8|||||||||
20650|Wright Hill Formation|62453|6|Mentioned|p50|||Underlies Punkerri Sandstone disconformably.||||||
20650|Wright Hill Formation|65102|4|Described|p365,366 Fig. 4-41; p.372, Table 4-15|Neoproterozoic|Neoproterozoic|Officer Basin. Laterally equivalent to Madley and Browne Formations. 500-3400m, siltstone, sandstone, quartzite; minor black oolitic chert; shallow marine; conformably overlying Pindyin beds (S.A.), type section in S.A., Birksgate and Lindsay areas, 27deg 35min S, 131deg 00min E; unfossiliferous.||||||
20650|Wright Hill Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
20686|Wy-Uda Shale Member|37460|6|Mentioned|p141|||||||||
20686|Wy-Uda Shale Member|38978|6|Mentioned|p156|||||||||18-JAN-07
20708|Wye Worry Member|22741|5|Briefly described|P25, Table3 P14||Sakmarian|||||||
20708|Wye Worry Member|22753|6|Mentioned|p535|||||||||
20708|Wye Worry Member|22767|5|Briefly described|Table3 P16, P21||Early Permian|||||||
20708|Wye Worry Member|22776|4|Described|Table.3|Early Permian|Early Permian|Carolyn Formation.||||||24-NOV-08
20708|Wye Worry Member|30338|2|Defined|p101|Early Permian|Early Permian|||||||
20708|Wye Worry Member|30342|6|Mentioned|p103|||||||||
20708|Wye Worry Member|36224|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Carolyn Formation (Grant Group).  Sandstone, mudstone, minor conglomerate lenses.||||||01-FEB-05
20708|Wye Worry Member|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
20708|Wye Worry Member|36634|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
20708|Wye Worry Member|37914|4|Described|p449|||||||||08-FEB-10
20708|Wye Worry Member|38217|5|Briefly described|p269|||||||||02-NOV-15
20708|Wye Worry Member|41158|6|Mentioned|p162|||||||||
20708|Wye Worry Member|41315|6|Mentioned|p149|||||||||
20708|Wye Worry Member|41839|5|Briefly described|p27|||||||||
20708|Wye Worry Member|42547|5|Briefly described|p97|||of Carolyn Formation||||||
20708|Wye Worry Member|42613|5|Briefly described|P 10, Table 1, Fig.3|||||||||
20708|Wye Worry Member|43015|5|Briefly described|Table 1,p319|||Of Carolyn Formation.||||||24-NOV-08
20708|Wye Worry Member|43816|5|Briefly described|Fig.2,p88|||||||||
20708|Wye Worry Member|45153|6|Mentioned|App.4-61|||||||||
20708|Wye Worry Member|49644|5|Briefly described|Table|||||||||
20708|Wye Worry Member|64630|6|Mentioned|p35 ||Tastubian|Of the Carolyn Formation. Probably correlates lithostratigraphically with Deeadeea Claystone Member and Ngumban Sandstone Member, all Carolyn Formation. Also correlated (using brachiopod fauna) with Calytrix Formation. Age: Tastubian faunal zone, Early Sakmarian.||||||12-SEP-13
20708|Wye Worry Member|64643|5|Briefly described|p8, p21|Sakmarian|Sakmarian|Of Carolyn Formation. Poorly exposed siltstone with dropstones. Overlain by Millajiddee Member.||||||
20708|Wye Worry Member|64974|5|Briefly described|p148 Fig. 6|Sakmarian|Sakmarian|Of Carolyn Formation (Grant Group). Geological Province: Canning Basin.||||||24-JUN-09
20708|Wye Worry Member|66949|4|Described|p57 App.3, p10-12, p13-14, p16, p18-19|Sakmarian|Sakmarian|See also p77,80-81 Appx.5. Type section detailed. Up to 95m thick; glacial lacustrine to shallow marine deposits. Contains trace fossils and (locally) brachiopods and pelecypods. Striking exposures in central Grant Range of striae directed to the NW.||Unit in Carolyn Formation.|||Diamictite, claystone/siltstone with dropstones, sandstone.|02-NOV-15
20708|Wye Worry Member|72497|4|Described|p1, p4-5, p7-9, p11-12, p18, p24-26.|Sakmarian|Sakmarian|Shown in Fig. 3, p4 as occurring towards the top of the Carolyn Formation, but described  as 'basal' on p5. Fluvioglacial to deltaic setting in a shallow-marine environment.Dropstones are common within the Late parts of this member. See also p28.||Carolyn Formation||Overlies Grant Group. Transitionally overlain by Millajiddee Member.|Light-brown to white, well-sorted, fine-grained quartzarenite and quartz wacke. Dropstones are present, especially in upper part.|
20708|Wye Worry Member|73117|5|Briefly described|p23, p117|||Of Crowe and Towner (1975). Exposed within the Saint George Ranges. 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||Overlain by Millajiddee Member.|Shaly diamictite and mudstone.|
20715|Wyloo Group|22484|6|Mentioned|p72|||||||||
20715|Wyloo Group|22743|6|Mentioned|p509|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20715|Wyloo Group|22816|6|Mentioned|p15 Fig.7|||||||||
20715|Wyloo Group|22837|6|Mentioned|Fig.1 p412|||||||||
20715|Wyloo Group|23045|5|Briefly described|289|||Age 2209 +/-15-1900 Ma||||||
20715|Wyloo Group|23047|6|Mentioned|34|||Hamersley Province.||||||10-FEB-09
20715|Wyloo Group|23280|6|Mentioned|p1084,Fig1p1085|||||||||
20715|Wyloo Group|23325|5|Briefly described|map legend|Precambrian|Precambrian|||||||
20715|Wyloo Group|23403|6|Mentioned|p3|||||||||
20715|Wyloo Group|23485|6|Mentioned|p16|||||||||
20715|Wyloo Group|23525|6|Mentioned|p8|||||||||
20715|Wyloo Group|23529|5|Briefly described|p10|||||||||
20715|Wyloo Group|23570|5|Briefly described|p14|Paleoproterozoic|Archean|Geological Province: Ashburton Basin||||||07-NOV-08
20715|Wyloo Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
20715|Wyloo Group|23612|4|Described|p841|Proterozoic|Proterozoic|Of Mount Bruce Supergroup [NO.Overlies Mt Bruce Supergroup]. Geological Province: Hamersley Basin [NO. Ashburton Basin]||||||23-NOV-10
20715|Wyloo Group|23723|5|Briefly described|p5|||Geological Province: Ashburton Basin.||||||
20715|Wyloo Group|23744|6|Mentioned|p3|||||||||
20715|Wyloo Group|23755|6|Mentioned|p10|||Of Mount Bruce Supergroup.||||||
20715|Wyloo Group|23774|5|Briefly described|p731|||Deposited in Ashburton Basin.||||||
20715|Wyloo Group|23781|6|Mentioned|p61|||||||||
20715|Wyloo Group|23890|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
20715|Wyloo Group|24017|5|Briefly described|p13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20715|Wyloo Group|24041|5|Briefly described|p492 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20715|Wyloo Group|24115|5|Briefly described|p5 Fig.3|||Geological Province: Ashburton Basin.||||||
20715|Wyloo Group|24183|5|Briefly described|p2 Fig.1, p6|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
20715|Wyloo Group|24203|5|Briefly described|p292 Fig. 7|||Age: 2200-1845 Ma.   Geological Province Carnarvon Basin.  See also p295.||||||
20715|Wyloo Group|24426|5|Briefly described|p217|Paleoproterozoic|Archean|Age: >2200 Ma. Geological Province: Hamersley Province.||||||07-FEB-11
20715|Wyloo Group|24544|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Mainly turbiditic sediments. Unconformably overlies Mount Bruce Supergroup. Geological Province: Ashburton Basin.||||||07-NOV-08
20715|Wyloo Group|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Geological Province: Pilbara Craton||||||
20715|Wyloo Group|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt. See also p853.||||||
20715|Wyloo Group|24607|5|Briefly described|p967, p969 Fig. 2|||Geological Province: Ashburton Basin. Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite, Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation||||||30-NOV-10
20715|Wyloo Group|29596|6|Mentioned|Table 1|||||||||
20715|Wyloo Group|29629|5|Briefly described|p899|||||||||
20715|Wyloo Group|29716|4|Described|Table 1|||||||||
20715|Wyloo Group|29845|6|Mentioned|p159|||||||||
20715|Wyloo Group|29848|6|Mentioned|p414|||||||||
20715|Wyloo Group|30482|6|Mentioned|p170|||||||||
20715|Wyloo Group|30488|6|Mentioned|p91|||Refers Compston & Arriens (1968) 2020 +/- 165 m.y.||||||
20715|Wyloo Group|30490|6|Mentioned|p108|||||||||
20715|Wyloo Group|30704|5|Briefly described|p59|||||||||
20715|Wyloo Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
20715|Wyloo Group|31393|6|Mentioned|Pl.25|||||||||
20715|Wyloo Group|31670|6|Mentioned|p911|||||||||
20715|Wyloo Group|31671|6|Mentioned|p9|||||||||
20715|Wyloo Group|31819|6|Mentioned|p80|||Part of Mt. Bruce Subgroup.||||||
20715|Wyloo Group|31828|6|Mentioned|p37|||Map. Proterozoic||||||
20715|Wyloo Group|31876|6|Mentioned|p11|||||||||
20715|Wyloo Group|32586|6|Mentioned|p113|||||||||
20715|Wyloo Group|32722|6|Mentioned|Fig.2|||Stromatolite||||||
20715|Wyloo Group|32727|6|Mentioned|Fig.17|||||||||
20715|Wyloo Group|32954|6|Mentioned|p184|||||||||
20715|Wyloo Group|33538|6|Mentioned|Fig.1|||||||||
20715|Wyloo Group|33540|6|Mentioned|Fig.2|||||||||
20715|Wyloo Group|33541|6|Mentioned|p103|||||||||
20715|Wyloo Group|33542|6|Mentioned|p411|||||||||
20715|Wyloo Group|33543|5|Briefly described|p132|||||||||
20715|Wyloo Group|33544|5|Briefly described|p30|||See also PP31, 34. Precambrian age||||||
20715|Wyloo Group|33545|5|Briefly described|p112|||||||||
20715|Wyloo Group|33630|6|Mentioned|Table 1|||||||||
20715|Wyloo Group|34022|6|Mentioned|p89|||? metamorphorised equivalent||||||
20715|Wyloo Group|34025|6|Mentioned|p49|||L.Proterozoic||||||
20715|Wyloo Group|34066|4|Described|p7|||L.Prot. See also P8||||||
20715|Wyloo Group|34115|6|Mentioned|p383|||Age||||||
20715|Wyloo Group|34124|4|Described|p3|||See also PP5,11,12 etc. Lower Proterozoic||||||
20715|Wyloo Group|34135|5|Briefly described|Table 2|||Lower Proterozoic||||||
20715|Wyloo Group|34287|6|Mentioned|p34|||See also PP36,37||||||
20715|Wyloo Group|34834|6|Mentioned|p212|||||||||
20715|Wyloo Group|35025|6|Mentioned|p142|||||||||
20715|Wyloo Group|35052|6|Mentioned|p18|||||||||
20715|Wyloo Group|35176|6|Mentioned|p12|||Petrology of volcanic rocks.||||||
20715|Wyloo Group|35218|4|Described|p6|||||||||
20715|Wyloo Group|35260|4|Described|p17|||||||||
20715|Wyloo Group|35269|6|Mentioned|p304|||||||||
20715|Wyloo Group|35495|6|Mentioned|p342|||||||||
20715|Wyloo Group|35639|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
20715|Wyloo Group|35949|6|Mentioned|Fig.8|||||||||
20715|Wyloo Group|35975|6|Mentioned|p106|||||||||
20715|Wyloo Group|35976|2|Defined|p107|Proterozoic|Proterozoic|||||||14-JUL-20
20715|Wyloo Group|36003|5|Briefly described|p1027|||||||||
20715|Wyloo Group|36247|6|Mentioned|p186|||See also Fig.2.||||||
20715|Wyloo Group|36257|6|Mentioned|p29|||||||||
20715|Wyloo Group|36308|6|Mentioned|p206|||||||||
20715|Wyloo Group|36551|6|Mentioned|Table 23|||||||||
20715|Wyloo Group|36642|6|Mentioned|Fig.1|||||||||
20715|Wyloo Group|36870|6|Mentioned|p61|||||||||
20715|Wyloo Group|36880|3|Fully described|p108|||||||||
20715|Wyloo Group|36882|3|Fully described|p135|||||||||
20715|Wyloo Group|36883|6|Mentioned|p143|||||||||
20715|Wyloo Group|36889|6|Mentioned|p217|||||||||
20715|Wyloo Group|36891|5|Briefly described|p441|||||||||
20715|Wyloo Group|36902|6|Mentioned|p15|||||||||
20715|Wyloo Group|37299|6|Mentioned|Fig.1|||||||||
20715|Wyloo Group|37327|4|Described|p396|||||||||
20715|Wyloo Group|37422|6|Mentioned|p8|||||||||
20715|Wyloo Group|37460|3|Fully described|p120|||||||||
20715|Wyloo Group|37577|6|Mentioned|p6|||||||||
20715|Wyloo Group|37704|6|Mentioned|Fig.2|||||||||
20715|Wyloo Group|37708|6|Mentioned|Fig.2|||||||||
20715|Wyloo Group|37934|6|Mentioned|p555|||||||||
20715|Wyloo Group|38243|6|Mentioned|Fig.2|||||||||
20715|Wyloo Group|38298|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20715|Wyloo Group|38299|6|Mentioned|p7|||||||||
20715|Wyloo Group|38321|6|Mentioned|Table 1|||||||||
20715|Wyloo Group|38326|6|Mentioned|p342|||||||||
20715|Wyloo Group|38482|6|Mentioned|p15|||See also P23.||||||
20715|Wyloo Group|38790|6|Mentioned|p162|||||||||
20715|Wyloo Group|38817|6|Mentioned|p168|||||||||
20715|Wyloo Group|38988|6|Mentioned|Fig.1|||||||||
20715|Wyloo Group|39162|6|Mentioned|p51|||||||||
20715|Wyloo Group|39200|6|Mentioned|Fig.1|||||||||
20715|Wyloo Group|39210|3|Fully described|p43|||See also Table 1||||||
20715|Wyloo Group|39427|6|Mentioned|p4|||||||||
20715|Wyloo Group|39697|6|Mentioned|p266|||||||||
20715|Wyloo Group|39894|6|Mentioned|p48|||||||||
20715|Wyloo Group|40089|6|Mentioned|p40|||See also P207||||||
20715|Wyloo Group|40103|6|Mentioned|p183|||||||||
20715|Wyloo Group|40105|6|Mentioned|p307|||||||||
20715|Wyloo Group|40369|6|Mentioned|p1|||See also Fig.1||||||
20715|Wyloo Group|40554|5|Briefly described|p29|||||||||
20715|Wyloo Group|40790|6|Mentioned|p193|||||||||
20715|Wyloo Group|40852|5|Briefly described|p22|||||||||
20715|Wyloo Group|40905|5|Briefly described|p70|||||||||
20715|Wyloo Group|40909|6|Mentioned|p19|||||||||
20715|Wyloo Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20715|Wyloo Group|40937|3|Fully described|p27|||||||||
20715|Wyloo Group|40938|6|Mentioned|p6|||||||||
20715|Wyloo Group|41125|6|Mentioned|p28|||||||||
20715|Wyloo Group|41243|4|Described|p258|||||||||
20715|Wyloo Group|41349|6|Mentioned|p1|||||||||
20715|Wyloo Group|41635|6|Mentioned|p19|||||||||
20715|Wyloo Group|41669|6|Mentioned|Table 3|||||||||
20715|Wyloo Group|41843|6|Mentioned|p67|||||||||
20715|Wyloo Group|41845|6|Mentioned|p81|||||||||
20715|Wyloo Group|41846|6|Mentioned|p94|||||||||
20715|Wyloo Group|41955|6|Mentioned|Fig.1 P4|||||||||
20715|Wyloo Group|41971|6|Mentioned|p342|||||||||
20715|Wyloo Group|42013|5|Briefly described|Map Legend|Proterozoic||||||||
20715|Wyloo Group|42020|5|Briefly described|p316|||||||||
20715|Wyloo Group|42148|5|Briefly described|p686|||See also Table 1||||||
20715|Wyloo Group|42190|6|Mentioned|Fig.4 Map|||||||||
20715|Wyloo Group|42260|5|Briefly described|p5|||||||||
20715|Wyloo Group|42277|6|Mentioned|p63|||||||||
20715|Wyloo Group|42343|6|Mentioned|p27|||||||||
20715|Wyloo Group|42435|6|Mentioned|p46|||||||||
20715|Wyloo Group|42471|5|Briefly described|p10|||Age about 2000 Ma||||||
20715|Wyloo Group|42686|5|Briefly described|map legend|Proterozoic||||||||
20715|Wyloo Group|42704|5|Briefly described|Plate 2E|Paleoproterozoic||Comprises Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite and Ashburton Formation.  Age: c.2000Ma.||||||07-NOV-08
20715|Wyloo Group|42730|6|Mentioned|p13|||||||||
20715|Wyloo Group|42744|3|Fully described|p6|||||||||
20715|Wyloo Group|42898|6|Mentioned|Fig.2 P341|||||||||
20715|Wyloo Group|43037|5|Briefly described|Table 1,p24.|||||||||
20715|Wyloo Group|43055|6|Mentioned|Table 3|||||||||
20715|Wyloo Group|43119|5|Briefly described|p13|||||||||
20715|Wyloo Group|43262|5|Briefly described|Map Legend||Proterozoic|||||||
20715|Wyloo Group|43290|4|Described|p8||Proterozoic|In Ashburton Basin. U-Pb zircon age of 1843 Ma,Pb-Pb age of about 2.0 Ga.||||||
20715|Wyloo Group|43561|6|Mentioned|p1433|||approx. 2500-2400 Ma||||||
20715|Wyloo Group|43595|4|Described|p75,219,343||Paleoproterozoic|Age: 2.0 Ga||||||07-NOV-08
20715|Wyloo Group|43644|6|Mentioned|p593|||||||||
20715|Wyloo Group|44111|6|Mentioned|p.56 Fig. 1|||||||||
20715|Wyloo Group|44141|6|Mentioned|p304||||2.0 Ga (Thorne).|||Is overlain unconformably by Bresnahan Group.||
20715|Wyloo Group|44142|6|Mentioned|p311 fig 4-15|||||||||
20715|Wyloo Group|44152|6|Mentioned|p179 Fig.2-155, p188 Fig.2-161, p189||||||Includes Beasley River Quartzite and Cheela Springs Basalt.|Overlies Turee Creek Group unconformably, locally conformably.||
20715|Wyloo Group|44319|14|Not recorded|map legend||Paleoproterozoic|Inc. Capricorn Fm., Ashburton Fm. & Duck Ck. Dolomite. L.Proterozoic.||||||07-NOV-08
20715|Wyloo Group|44477|4|Described|p.11-12, Table 1||Proterozoic|SF/50-6.||||||
20715|Wyloo Group|44478|14|Not recorded|map legend||Proterozoic|||||||
20715|Wyloo Group|44481|5|Briefly described|map legend||Proterozoic|||||||
20715|Wyloo Group|44503|14|Not recorded|p.8|||||||||
20715|Wyloo Group|44692|4|Described|p.6,7,Tb.1, map|||(F50-11). See also p.9,11,16-19,23, for more details.||||||
20715|Wyloo Group|44729|5|Briefly described|map legend|Proterozoic||Of Mount Bruce Supergroup.||||||
20715|Wyloo Group|44867|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20715|Wyloo Group|45086|5|Briefly described|p22|||Age. Lithology.||||||
20715|Wyloo Group|45965|14|Not recorded|p.58|||||||||
20715|Wyloo Group|46917|6|Mentioned|p172|||||||||
20715|Wyloo Group|50216|5|Briefly described|p208|Paleoproterozoic|Paleoproterozoic|Includes the Cheela Springs Basalt. Max. thickness: ~12 km. Geological Province: Ashburton Basin.||||||07-NOV-08
20715|Wyloo Group|50222|6|Mentioned|p327|||Includes the Duck Creek Dolomite.  Age: <1.84Ga (Pidgeon and Horwitz, 1991).||||||
20715|Wyloo Group|50225|5|Briefly described|p386 Fig. 1, p388|||||||||07-FEB-11
20715|Wyloo Group|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Mount Bruce Supergroup.  Age: 2.2Ga (Martin et al, 2000).  Intruded by the Boolaloo Granodiorite.  Geological Province: Asburton Basin.||||||07-NOV-08
20715|Wyloo Group|50227|6|Mentioned|p445|||Divided into Upper and Lower Wyloo Groups for most of this study.||||||07-FEB-11
20715|Wyloo Group|50380|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin. Age: < 1840 Ma||||||07-NOV-08
20715|Wyloo Group|50425|6|Mentioned|p2.1|||||||||
20715|Wyloo Group|50549|5|Briefly described|p1159 Fig.2|||||||||
20715|Wyloo Group|60301|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Asburton Formation. Age: c. 1806Ma. Geological Province: Ashburton Basin.||||||
20715|Wyloo Group|60539|5|Briefly described|p498 Fig.1|||Geological Province: Pilbara Craton. Overlies Mount Bruce Supergroup.||||||
20715|Wyloo Group|61268|6|Mentioned|p77|||Geological Province: Ashburton Basin||||||
20715|Wyloo Group|61276|5|Briefly described|p577-580|Orosirian|Orosirian|Geological Province: Ashburton Province. Includes a stratigraphic break between the Wooly Dolomite and Mount McGrath Formation, informally dividing the group into Lower and Upper parts.  Base age ~2045. Ages ~ 2031 Ma from Wooly Dolomite and 1829 +/- 5Ma from volcanics in Ashburton Fm.||||||17-OCT-16
20715|Wyloo Group|61526|6|Mentioned|p880|||See also Upper and Lower Wyloo Groups. Includes Beasley River Quartzite, Cheela Springs Basalt and Wooly Dolomite.||||||
20715|Wyloo Group|62129|3|Fully described|p13, p13 Fig. 1, p14, p16-20, p22|Proterozoic|Proterozoic|Includes; Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation. Age: 2000 (Pb isotopes) and 1843 ( U-Pb) Ma. Geological Province: Ashburton Basin.||||||07-FEB-11
20715|Wyloo Group|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite and Ashburton Formation. Geological Province: Ashburton Basin.||||||
20715|Wyloo Group|62289|6|Mentioned|p4|||||||||
20715|Wyloo Group|63153|5|Briefly described|p1359,|||||||Unconformably overlies the Mount Bruce Supergroup.||
20715|Wyloo Group|63246|5|Briefly described|p478 Fig. 1|||Includes the Ashburton Formation.||||||
20715|Wyloo Group|63432|5|Briefly described|p735 Fig. 1, p736 Fig. 2|Proterozoic|Proterozoic|Geological Province: Pilbara Craton.||||||07-FEB-11
20715|Wyloo Group|63866|5|Briefly described|p151, p154, p168|Proterozoic|Proterozoic|Ashburton Basin, Capricorn Orogen. Up to 12km thick.||||Unconformably overlies the Turee Creek Group (Mount Bruce Supergroup). Overlain by the Capricorn Group.|Low-grade sedimentary and volcanic rocks.|
20715|Wyloo Group|63869|4|Described|p1, p4-7, p10, p12, p14, p16, p28, p29|Paleoproterozoic|Paleoproterozoic|See also p45, p47, p49, Plate 1. Informally established and subdivided by MacLeod et al. (1963); revised by Trendall (1979), Horwitz (1980) and Thorne and Seymour (1991). Ashburton Fold Belt, Ashburton Basin. 12 km thick. Deformed.|2446-1786 Ma.||Includes Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics and Ashburton Formation.|Overlies Turee Creek Group. Is overlain by Capricorn Group.|Undivided: siltstone, mudstone, sandstone, dolostone, conglomerate, felsic and mafic volcanic rock, BIF; lower greenschist facies.|
20715|Wyloo Group|64284|6|Mentioned|p59|||Written as upper Wyloo Group. Contains Duck Creek Dolomite.||||||07-FEB-11
20715|Wyloo Group|64384|5|Briefly described|p1, p41 Fig. 35, p47 Tb. 7, p78|||Comprises Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Fm., Duck Creek Dolomite+Ashburton Fm; June Hill Volcanics locally in upper part of group. Geol.province: Ashburton Basin. Compared with interpretation of Glengarry Group by author||||||07-FEB-11
20715|Wyloo Group|64580|4|Described|map legend||Paleoproterozoic|Lower: Congl, sandst, mudst, basalt, chert, local stromatolitic dolomite. Includes BEASLEY RIVER QUARTZITE, CHEELA SPRINGS BASALT, WOOLY DOLOMITE. Upper: wacke, mudst, BIF, chert, sandst, congl, felsic and mafic volcanics, local stromatolitic dolomite.||||||09-DEC-08
20715|Wyloo Group|64722|5|Briefly described|Fig. 2 p3-6, p7, 23|Orosirian|Rhyacian|Unit of the 2200 - 1805 Ma Ashburton Basin. Overlain by Blair Basin succession.||||Overlies Turee Creek Group.||11-APR-12
20715|Wyloo Group|64724|6|Mentioned|p43, p45 Fig.5|Orosirian|Orosirian|Ashburton Basin||||||02-APR-12
20715|Wyloo Group|64728|5|Briefly described|p94 Fig.1, p95, pp106-107.|||Low-grade metasedimentary rocks. 12 km thick. Intruded by granites of the Moorarie Supersuite between 1830 Ma and 1780 Ma. Contains detrital zircons derived from Mount Bruce Supergroup and Pilbara Craton.|Lower portion deposited between c.2209-2031 Ma.||Includes Ashburton and Mount McGrath Formations and Beasley River Quartzite.|Overlies Mount Bruce Supergroup. Is unconformably overlain by Bangemall Supergroup.||
20715|Wyloo Group|64872|6|Mentioned|p24 Fig.1|||Includes Ashburton Formation.||||||
20715|Wyloo Group|65152|6|Mentioned|p2 Fig.1.|||Includes Ashburton Formation.||||||
20715|Wyloo Group|65194|5|Briefly described|p98 Fig.4.23|||||||||11-APR-16
20715|Wyloo Group|65506|6|Mentioned|p987 Fig.1A|||||||||
20715|Wyloo Group|65830|5|Briefly described|p3, p4, p12, p24, p25, p26 Fig.13|||See also Plates 1,2. The Ashburton Basin corresponds to the present-day outcrop of this unit. ~ 12km thick. Consists of an upper and lower succession.|||Includes Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics and Ashburton Formation.|Overlain by the Capricorn Group.|Succession of low-grade, metasedimentary and metavolcanic rocks.|
20715|Wyloo Group|66115|5|Briefly described|p136, p137 Fig.1|Paleoproterozoic|Paleoproterozoic||||Ashburton Formation, June Hill Volcanics, Mount McGrath Formation, Cheela Springs Basalt, Beasley River Quartzite|Disconformably overlies Mount Bruce Supergroup. Is overlain by Ashburton|Contains two carbonate platforms capped by volcanics and a thick siliciclastic succession; metamorphosed.|
20715|Wyloo Group|66217|5|Briefly described|p44.|Paleoproterozoic|Paleoproterozoic||2200-1800 Ma.|||Unconformably overlies Mount Bruce Supergroup.||
20715|Wyloo Group|66299|5|Briefly described|p3, p202.|Paleoproterozoic|Paleoproterozoic|Ashburton Fold belt.|||Includes Ashburton Formation.|||
20715|Wyloo Group|66359|6|Mentioned|e96|||Unconformably overlies Turee Creek Group. Cheela Springs Basalt near base of Wyloo Group is dated as 2209 +/-15 Ma.||||||19-SEP-13
20715|Wyloo Group|66427|6|Mentioned|p47, |||||||||
20715|Wyloo Group|66574|4|Described|p911, p912 Fig.1, p916-918 Figs.4-6|Orosirian||Divided into lower and upper, contains Wooly Dolomite and Cheela Springs Basalt. Unconformably overlies Mount Bruce Supergroup.||||||
20715|Wyloo Group|66950|5|Briefly described|p2, p4, p5, p6, p11, p12, p13|Rhyacian|Rhyacian|Geochronology of baddeleyite from mafic dykes and sills in the lower Wyloo Group.|c. 2210-2030 Ma (Muller et al. 2005).||Includes the Beasley River Quartzite, Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics, and Ashburton Formation.|Underlain by the Turee Creek Group. Intruded by the Moorarie Supersuite.||
20715|Wyloo Group|67025|4|Described|p319, p320 Table 1, pp323-324, p328.|Paleoproterozoic|Paleoproterozoic|Formed after the c. 2200 Ma Ophthalmian Orogeny. Thickness about 10 - 12 km. There exists a regional remanent magnetic overprint directed moderately upwards to the northwest in the lower units of this Group.|c. 2200 - c. 1843 Ma.||Includes Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite and Ashburton Formation.|Unconformably overlies the Mount Bruce Supergroup.||
20715|Wyloo Group|67056|5|Briefly described|p423.||||||Includes Lower and Upper units.||Includes a BIF jasper-rich type pebble conglomerate with occasional ore pebbles.|
20715|Wyloo Group|67130|5|Briefly described|p1, p24 fig 17|Statherian|Rhyacian|Ashburton Basin. Approximately 12km thick. Divided into unconformity-bound upper and lower parts.|2200 Ma - 1800 Ma|||Unconformably overlies Turee Creek Group, Unconformably  overlain by Bangemall Group|Low grade sedimentary and volcanic rocks.|
20715|Wyloo Group|67136|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|||Includes Ashburton Formation.|||
20715|Wyloo Group|67201|5|Briefly described|p33 Fig.17, p35|||Ashburton Basin. Angular unconformity at base of lower Wyloo Group. Shown as Lower Wyloo Group in Fig.19.|||Cheela Springs Basalt in lower Wyloo Group|||
20715|Wyloo Group|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|||Includes Ashburton Formation.|||
20715|Wyloo Group|67721|5|Briefly described|p37, p38 Fig.9|Orosirian|Orosirian|Upper: > 5000-10000 m thick; Lower: 10000-12000 m thick.|c. 2008-1850 Ma||Includes Mount McGrath Formation.|||
20715|Wyloo Group|67829|5|Briefly described|p447, p451. |||Hamersley Province. Includes iron ore-bearing conglomerates.|||Includes Mount McGrath Formation and Beasley River Quartzite.|Unconformably overlies the Hamersley BIFs.||
20715|Wyloo Group|67843|5|Briefly described|p3, p33.|Paleoproterozoic|Paleoproterozoic|This unit covers a suture between the Glenburgh Terrane and Pilbara Craton, indicating they collided before this date.|c.1830 Ma (Sircombe 2003).||Includes Ashburton Formation, Beasley River Quartzite, Cheela Springs Basalt.|||
20715|Wyloo Group|67855|5|Briefly described|p210-212, 220, 223-4, 228-9, 230 |Paleoproterozoic|Paleoproterozoic|Of Ashburton Basin. Age poorly known. Max age from Woongarra Volcanics clasts in base of group 2470 +/-30 Ma U-Pb zircon age (Compston et al.1981). See also p198-199, 202, 218|~2000 Ma||Includes Ashburton Formation, June Hill Volcanics, Duck Creek Dolomite, Mount McGrath Formation, Wooly Dolomite, Cheela Springs Basalt, Beasley River Quartzite.|Unconformably overlies Turee Creek Group, Mount Bruce Supergroup.||
20715|Wyloo Group|67888|6|Mentioned|p52||||||Includes Ashburton Formation|||
20715|Wyloo Group|68035|4|Described|p292, 283, 284 Fig 1|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Thickness ~12 km (Thorne and Seymour, 1991). Divided into unconformity-bound upper (1.83 - 1.79 Ga) and lower parts, the lower part resting unconformably on the Hamersley Basin, and the upper part unconformably overlain by younger Proterozoic basins.|||Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite, Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation.||Low-grade sedimentary and volcanic rocks.|
20715|Wyloo Group|68280|6|Mentioned|p1, p5, p48, p54|Paleoproterozoic|Paleoproterozoic||||Includes Ashburton Formation, June Hill Volcanics, Duck Creek Dolomite, Mt McGrath Formation, Wooly Dolomite, Cheela Springs Basalt|Overlies Turee Creek Group||
20715|Wyloo Group|68285|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton Basin.|||Includes the Ashburton Formation.|Unconformably overlain by Bresnahan Group or Edmund Group.||
20715|Wyloo Group|68286|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton Basin.|||Includes the Ashburton Formation.|Unconformably overlain by Edmund Group.||
20715|Wyloo Group|68981|5|Briefly described|p20-21|||Thorne and Seymour (1991). Ashburton Basin. Deposition associated with the 1820-1770 Ma Capricorn Orogeny. The upper part of this unit is mostly a turbiditic deep-marine succession, deformed once.|c.2200-c.1800 Ma.||Ashburton Formation.|Is overlain unconformably by the Capricorn Group.||
20715|Wyloo Group|69003|5|Briefly described|p4, p7-8, p9 Fig.9|||Capricorn Orogen. Retro-foreland basin deposits from the eroded Ophthalmia Fold Belt. Lower part is up to 3km thick. Also appears as lower and upper Wyloo Group.||||||
20715|Wyloo Group|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. See map legend for a detailed lithological description. Geochronology obtained from an unnamed felsic volcaniclastic unit in the middle of the Group.|c. 1806-1829 Ma (GSWA, in prep; Sircombe, 2003)||Includes the Ashburton Formation and the Duck Creek Dolomite.||Includes sandstone, siltstone, conglomerate, felsic volcanic rock, and laminated dolostone.|
20715|Wyloo Group|69027|6|Mentioned|Map Legend|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|||Includes the Ashburton Formation.|Overlain by the Edmund Group.||
20715|Wyloo Group|69080|4|Described|p684, p687-689, p691-699|||Ashburton Basin, Pilbara Craton. Thickness c.10.5 km.|||Includes Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics, Ashburton Formation.|Unconformably overlies Turee Creek Group.|Quartzite, basalt and dolomite in lower parts; wacke, mudstone, BIF, chert, sandstone, conglomerate, bimodal volcanics, local stromatolitic dolomite in upper parts.|
20715|Wyloo Group|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Ashburton Formation, Duck Creek Dolomite, Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite||Undivided; mudstone; sandstone, basalt, chert, locally stromatolitic dolomite, wacke, ferruginous mudstone, banded iron formation, conglomerate; felsic and mafic volcanic rocks.|
20715|Wyloo Group|69185|4|Described|GEOL_LUT_CSV files||Paleoproterozoic|Of Ashburton Basin.|c. 1840 Ma||Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.||Wacke, mudstone, ferruginous mudstone, banded iron-formation, basalt, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|
20715|Wyloo Group|69237|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic||||Ashburton Formation.|||
20715|Wyloo Group|69387|5|Briefly described|p3, p6-7, p19, p33-34|Orosirian|Orosirian|Ashburton Basin, Gascoyne Province. Structural fabric diagram. Gravity and magnetic modelling.|1830-1800 Ma.|||||
20715|Wyloo Group|69538|5|Briefly described|p517 Fig.3, p520, p522 Fig.5, p533|Paleoproterozoic|Paleoproterozoic||||Includes Beasley River Quartzite; Cheela Springs Basalt; Wooly, Duck Creek Dolomites; Mount McGrath, Ashburton Formations; June Hill Volcanics.|Overlies Turee Creek Group.||
20715|Wyloo Group|69546|6|Mentioned|p102|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province.||||||
20715|Wyloo Group|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.|||Beasley River Quartzite, Cheela Springs Basalt, Mount McGrath Formation.|Overlies Turee Creek Group (Mount Bruce Supergroup).||
20715|Wyloo Group|69583|6|Mentioned|p132||||||Beasley River Quartzite.|||
20715|Wyloo Group|69596|6|Mentioned|p1, p4, p7|||Ophthalmia Fold Belt, Capricorn Orogen. See also references to Wyloo Group, Lower (p5-7, p8 Fig.5) and Upper (p5, p8 Fig.5).||||||
20715|Wyloo Group|69745|6|Mentioned|p270, 272-273, 287, 289-290|||Hamersley Province.||||Unconformably overlies Turee Creek Group (Mount Bruce Supergroup). Is overlain unconformably by Upper Wyloo Group.||
20715|Wyloo Group|69754|6|Mentioned|p316-p317, p336, p340-p341|||Pilbara Craton. Metamorphosed to the Prehnite-pumpellyite-epidote facies.|||Includes the Beasley River Quartzite, Cheela Springs Basalt and Ashburton Formation.|||
20715|Wyloo Group|70086|5|Briefly described|p195-196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.|||Includes Mount McGrath Formation, Cheela Springs Basalt and Beasley River Quartzite.|Underlain unconformably by Mount Bruce Supergroup/Turee Creek Group.||
20715|Wyloo Group|70327|6|Mentioned|p2, p4, p17|||Ashburton Province.|||Lower Wyloo Group, Wooly Dolomite.|||
20715|Wyloo Group|70767|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|2008-1786 Ma.||Ashburton Formation.|Is overlain unconformably by Bresnahan Group.||
20715|Wyloo Group|70768|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|2008-1786 Ma.||Ashburton Formation.|Is overlain unconformably by Bresnahan Group.||
20715|Wyloo Group|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv,GA_geochron.csv, West Australian Craton|1806-1799 Ma||Includes Ashburton Formation, Duck Creek Dolomite||Sandstone, siltstone, mudstone, conglomerate, dolostone and mafic and felsic volcanic rocks; metamorphosed.|
20715|Wyloo Group|70814|5|Briefly described|p3-p4, p8, p32, p34-p35, p71|Paleoproterozoic|Paleoproterozoic|The former lower subdivision of this group is now the Shingle Creek Group.|2008-1706 Ma||Includes the Mount McGrath Formation and the Ashburton Formation.|Unconformably overlain by the Yilgatherra Formation and the Irregully Formation.||
20715|Wyloo Group|70826|6|Mentioned|p6 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. May be a time equivalent to the Miningarra Group.||||||
20715|Wyloo Group|70949|4|Described|p988-989, p998-1000|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Formerly the upper Wyloo Group; the lower part was hived off to form the Shingle Creek Group. Deposition occurred with the onset of early deformation of the 1820-1770 Ma Capricorn Orogeny. ~7.5 km thick.|||Mount McGrath, Ashburton Formations; Duck Creek Dolomite.|Overlies the Shingle Creek Group.|A metasedimentary sequence of wacke, mudstone, ferruginous mudstone, BIF, chert, sandstone, conglomerate, felsic and mafic volcanic rocks and, locally, stromatolitic dolomite.|
20715|Wyloo Group|70958|4|Described|p1, 4-7, Fig. 1|Paleoproterozoic|Paleoproterozoic|Changes facies and thickness from  a shelf environment to the Ashburton Trough.||||Unconformably overlies Mount Bruce Supergroup along shelf margin.||
20715|Wyloo Group|71112|6|Mentioned|p69,80|Paleoproterozoic|Paleoproterozoic|Geological province: Ashburton Province, Pilbara Craton. Intruded by a sill up to 30m from the base of the package.|~1.8 Ga|||||
20715|Wyloo Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, dolostone, basalt, siltstone, volcaniclastic rock, conglomerate, banded iron formation, greywacke, acid volcanic rock, chert, mudstone|
20715|Wyloo Group|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|c.2008-c.1796 Ma.||Mount McGrath, Ashburton Formations; Duck Creek Dolomite; June Hill Volcanics.|||16-FEB-18
20715|Wyloo Group|71513|6|Mentioned|p66 fig 1,|||Pilbara Craton.||||||
20715|Wyloo Group|71803|6|Mentioned|p367 fig 1|||||||||
20715|Wyloo Group|71869|6|Mentioned|p3|||Capricorn Orogen.|||Includes the Ashburton Formation.|||
20715|Wyloo Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|||Includes Ashburton Formation, June Hill Volcanics, Duck Creek Dolomite,  Mount McGrath Formation.||Sandstone, siltstone, pebbly sandstone, conglomerate, and dolostone; minor mafic and felsic volcanic rocks and banded iron-formation; metamorphosed.|
20715|Wyloo Group|72254|6|Mentioned|App.A p11|||||||Unconformably underlain by Turee Creek Group.||
20715|Wyloo Group|72259|6|Mentioned|p3|Orosirian|Orosirian||ca. 1830-1800 Ma|||||
20715|Wyloo Group|72447|6|Mentioned|p238|||||||||
20715|Wyloo Group|72570|6|Mentioned|p3 fig 1||||||Includes the Ashburton Formation, June Hill Volcanics, Duck Creek Dolomite and the Mount McGrath Formation.|||
20715|Wyloo Group|72712|4|Described|p1, p3, p5, p9, p25, p31, p33-34.|Statherian|Orosirian|Revised. Includes only units form the informal 'upper Wyloo Group'. The revised Wyloo Group is not described in detail in this report. Most of the 'lower Wyloo Group' now included in the Shingle Creek Group. See also p39, p45, p52-53, p63, p2 Fig.1. Shown on p63 (Report No. 203 back cover summary).|c. 2008 Ma to 1786 +/- 11 Ma.||Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics and Ashburton Formation.|Shown as unconformably overlying Turee Creek Group and Wooly Formation. Faulted against the Shingle Creek Group.||14-JAN-21
20715|Wyloo Group|72758|4|Described|p4 Tb.1, p27, p29-41, p43, p45,|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Maximum thickness 10-12km. Age poorly constrained by underlying Hamersley Group rocks (2470+/-30 Ma) and granite intruding Ashburton Formation (top of group) with Rb-Sr mineral isochron of 1680 Ma. Informally subdivided into lower Wyloo Group, and upper Wyloo Group (Ashburton Formation). Includes submarine-fan and associated basin-plain sediments with shallow-marine shelf deposits. Includes volcanics confined to area north of the Wyloo Dome. See also p48, p54-55, p59.|Age range ~ 2470 - 1680 Ma||Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite, Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics, Ashburton Formation|Unconformably overlies Mount Bruce Supergroup and unconformably underlies Mount Minnie and Bangemall Groups.|Includes silicified quartz sandstone, local BIF derived conglomerate, mudstone, and carbonate. Vesicular and amygdaloidal basalt with minor tuff, chert and dolerite sills. Includes arenite, wacke, relic evaporite textures and dolomitic breccias.|
20715|Wyloo Group|73022|6|Mentioned|p2 Fig.1|||||||||
20715|Wyloo Group|73102|6|Mentioned|p20|||||||Intruded by Kulkatharra Dolerite.||
20715|Wyloo Group|73538|6|Mentioned|p2 Fig. 1, p3|||Basal unit is the Beasley River Quartzite.||||Unconformably underlain by the Turee Creek Group including the Kazput Formation.|Includes carbonates, mafic volcanics, and quartzite.|
20715|Wyloo Group|75075|6|Mentioned|p420 Fig.1, 424|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||||||
20719|Wyndham Shale|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20719|Wyndham Shale|32660|5|Briefly described|Table 3|||||||||
20719|Wyndham Shale|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
20719|Wyndham Shale|32728|6|Mentioned|Table 5|||||||||
20719|Wyndham Shale|34462|6|Mentioned|p9|||Refers Lissadell sheet||||||
20719|Wyndham Shale|36551|6|Mentioned|Table 10|||||||||
20719|Wyndham Shale|36885|4|Described|p185|||||||||
20719|Wyndham Shale|41811|6|Mentioned|p213|||||||||
20719|Wyndham Shale|44140|5|Briefly described|p294|Paleoproterozoic|Paleoproterozoic|700 m thick.||Bastion Group|||Green shale, siltstone, sandstone, calcareous sandstone; mud cracks, ripple bedding; black calcite nodules.|
20719|Wyndham Shale|44230|5|Briefly described|Map Legend|Mesoproterozoic|Statherian|Bastion Group||||||25-NOV-08
20719|Wyndham Shale|44363|5|Briefly described|p.6,10,12,16|||(Carpentarian) Bastion Group.||||||
20719|Wyndham Shale|44364|14|Not recorded|map legend||Proterozoic|Unit of Bastion Group.||||||
20719|Wyndham Shale|45047|5|Briefly described|p28|||||||||
20719|Wyndham Shale|64748|5|Briefly described|p275|Orosirian|Statherian|Of the Bastion Group; whole-rock Rb-Sr date of 1789+/-58Ma||||||
20719|Wyndham Shale|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Bastion Group.|||Green and grey shale and siltstone with fine-grained sandstone interbeds|
20744|Yagahong beds|38994|6|Mentioned|Fig.1|||||||||
20750|Yakabindie Metadunites|38459|6|Mentioned|p1559|||||||||
20814|Yandicoogina Shale Member|23126|5|Briefly described|p383 Fig.3|||||||||
20814|Yandicoogina Shale Member|23536|5|Briefly described|Fig 2 p 429|||||||||
20814|Yandicoogina Shale Member|24041|5|Briefly described|p492|Paleoproterozoic|Archean|Of the Brockman Iron Formation.||||||07-NOV-08
20814|Yandicoogina Shale Member|24231|5|Briefly described|p186 Fig.2|||Geological Province: Hamersley Basin.||||||
20814|Yandicoogina Shale Member|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Brockman Iron Formation. Overlies Joffre Member. Overlain by Weeli Wooli Formation. Geological Province: Hamersley Province.||||||07-FEB-11
20814|Yandicoogina Shale Member|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Brockman Iron Formation. Overlies Joffre Member. Overlain by Weeli Wolli Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
20814|Yandicoogina Shale Member|29629|5|Briefly described|p899|||||||||
20814|Yandicoogina Shale Member|29716|4|Described|Table 1|||||||||
20814|Yandicoogina Shale Member|31671|5|Briefly described|p11|||||||||
20814|Yandicoogina Shale Member|32326|6|Mentioned|p122|||Hamersley Gp.||||||
20814|Yandicoogina Shale Member|33542|6|Mentioned|p412|||||||||
20814|Yandicoogina Shale Member|33544|2|Defined|p80|Proterozoic|Proterozoic|See also P81||||||
20814|Yandicoogina Shale Member|33545|5|Briefly described|p113|||||||||
20814|Yandicoogina Shale Member|33687|5|Briefly described|p918|||Also P921 re mineralization||||||
20814|Yandicoogina Shale Member|34541|6|Mentioned|p53|||See also P54||||||
20814|Yandicoogina Shale Member|34542|6|Mentioned|p94|||Overlies Joffre Member||||||
20814|Yandicoogina Shale Member|35052|6|Mentioned|Fig.2|||||||||
20814|Yandicoogina Shale Member|35260|6|Mentioned|Fig.4|||||||||
20814|Yandicoogina Shale Member|36247|6|Mentioned|Fig.2|||||||||
20814|Yandicoogina Shale Member|36260|5|Briefly described|p78|Paleoproterozoic|Paleoproterozoic|Of the Brockman Iron Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
20814|Yandicoogina Shale Member|36642|6|Mentioned|Table 1|||||||||
20814|Yandicoogina Shale Member|36882|4|Described|p134|||||||||
20814|Yandicoogina Shale Member|37297|6|Mentioned|Fig.2|||||||||
20814|Yandicoogina Shale Member|37460|6|Mentioned|Fig.3.4|||||||||
20814|Yandicoogina Shale Member|37704|6|Mentioned|Fig.1|||||||||
20814|Yandicoogina Shale Member|37708|6|Mentioned|p1930|||||||||
20814|Yandicoogina Shale Member|38790|6|Mentioned|p164|||||||||
20814|Yandicoogina Shale Member|39200|6|Mentioned|Fig.4|||||||||
20814|Yandicoogina Shale Member|39697|6|Mentioned|p126|||||||||
20814|Yandicoogina Shale Member|41358|5|Briefly described|p146|||||||||
20814|Yandicoogina Shale Member|41768|6|Mentioned|p28|||||||||
20814|Yandicoogina Shale Member|42112|5|Briefly described|p9|||See also Table 1||||||
20814|Yandicoogina Shale Member|42190|6|Mentioned|Fig.3 P273|||||||||
20814|Yandicoogina Shale Member|42471|4|Described|p8|||of Brockman Iron Formation||||||
20814|Yandicoogina Shale Member|42495|6|Mentioned|p35|||||||||
20814|Yandicoogina Shale Member|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
20814|Yandicoogina Shale Member|42744|4|Described|p5|||of Brockman Iron Formation.||||||
20814|Yandicoogina Shale Member|43119|5|Briefly described|p10|||of Brockman Iron Formation||||||
20814|Yandicoogina Shale Member|43210|5|Briefly described|Table 1 p3,p5.||Mesoproterozoic|of Brockman Iron Formation.||||||
20814|Yandicoogina Shale Member|43262|6|Mentioned|Map Legend||Proterozoic|of Hamersley Group.||||||
20814|Yandicoogina Shale Member|43290|5|Briefly described|p7||Proterozoic|of Brockman Iron Formation.||||||
20814|Yandicoogina Shale Member|43595|6|Mentioned|Fig.2-49,p220|||||||||
20814|Yandicoogina Shale Member|44152|5|Briefly described|p178, p179 Fig.2-155|||The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Brockman Iron Formation||Overlies Joffre Member. Is overlain by Weeli Wolli Formation.|Shale.|
20814|Yandicoogina Shale Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Brockman Iron Formation.||||||23-JUN-09
20814|Yandicoogina Shale Member|62129|3|Fully described|p10|Archaean|Archaean|Of Brockman Iron Formation. Overlies Joffre Member. Thickness: 40m. Geological Province: Hamersley Basin. Comprises alternating chert and thin shale, intruded by dolerite sills.||||||08-MAY-12
20814|Yandicoogina Shale Member|63153|6|Mentioned|p1362 Fig.3, |||||Unit in Brockman Iron Formation.||||
20814|Yandicoogina Shale Member|64406|5|Briefly described|p1-2|||Of the Brockman Iron Formation. Geological Province: Hamersley Basin.  Discussed in the context of its use as facing stone forming the lift panels in Mineral House, Perth.||||||
20814|Yandicoogina Shale Member|65683|5|Briefly described|p801 Fig2|||Of Brockman Iron Formation. Underlies Weeli Wolli Formation; overlies Joffre Member.||||||08-MAR-12
20814|Yandicoogina Shale Member|67025|5|Briefly described|p319.|||||Topmost unit in Brockman Iron Formation.||Conformably overlies Joffre Member. Is overlain conformably by Weeli Wolli Formation.||
20814|Yandicoogina Shale Member|67130|5|Briefly described|p3 fig 2, p8 fig 5|||||Brockman Iron Formation||Overlies Joffre Member, overlain by Woongarra Rhyolite, Weeli Wolli Formation.|Shale|
20814|Yandicoogina Shale Member|67201|6|Mentioned|p34 Fig.18|||||Brockman Iron Formation||||25-NOV-16
20814|Yandicoogina Shale Member|68035|5|Briefly described|p292 Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Group, Hamersley Basin.||Of Brockman Iron Formation.||Overlies Joffre Member. Overlain by Weeli Wolli Formation.|Shale.|
20814|Yandicoogina Shale Member|68280|5|Briefly described|p5|||||Brockman Iron Formation||Overlies Joffre Member|Shale.|
20814|Yandicoogina Shale Member|69538|6|Mentioned|p517 Fig.3|||Appears in Fig.3 as Yadicoogina Shale.||Unit in Brockman Iron Formation.||||
20814|Yandicoogina Shale Member|69745|6|Mentioned|p281|||Mount Wall area, Hamersley Province. Abbreviated (for reasons of space) to Yandi Shale Member.||Brockman Iron Formation.||||
20814|Yandicoogina Shale Member|70509|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton.||Unit of Brockman Iron Formation.||Uppermost unit of Brockman Iron Formation. Overlain by Weeli Wolli Formation. Underlain by Joffre Member.||
20814|Yandicoogina Shale Member|71808|4|Described|viii-ix, p30, p34-p35|||Hamersley Province. Typically poorly exposed as a dip slope on the back of the Joffre Member hills. Approximately 60m thick at the west end of Box Canyon. Authors suggest renaming to the Yandicoogina Member as shale is not the dominant lithology where it is best exposed. See also p39-p40, p45-p46, p107, p117, p209.||Brockman Iron Formation||Overlies the Joffre Member. Overlain by the Weeli Wolli Formation.|Wavy-banded, yellow and grey, microbanded red/yellow striped cherts with subordinate interbedded shale.|
20814|Yandicoogina Shale Member|72493|5|Briefly described|p30|||Hamersley Basin.||Brockman Iron Formation.||Overlies Joffre Member. Is overlain by Weeli Wolli Formation.|Shale.|
20814|Yandicoogina 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.|Probably top of Brockman Iron Formation.||Probably overlies the Joffre Member. Probably overlain by Weeli Wolli Formation.|Includes shale.|
20814|Yandicoogina Shale Member|72758|5|Briefly described|p15 Tb.1, p25.|||Present over much of northeastern WYLOO.||Brockman Iron Formation|||Banded iron formation and mudstone and black, laminated mudstone and contain subordinate chert and carbonate.|
20814|Yandicoogina Shale Member|73022|6|Mentioned|p3 Fig.2|||||Brockman Iron Formation||Overlies the Joffre Member, underlies the Weeli Wolli Formation.|Shale, minor Fe-chert and banded iron formation.|
20814|Yandicoogina Shale Member|73290|6|Mentioned|p784|||Hamersley Province.||||||
20814|Yandicoogina Shale Member|73538|6|Mentioned|p4|Siderian|Siderian|||Brockman Iron Formation||Underlain by Joffre Member. Overlain by Weeli Wolli Formation.|Mudstone/siltstone.|
20842|Yardarino Sandstone Member|23816|6|Mentioned|p235|||Synonymous with the "Yardarino Sandstone".||||||16-DEC-04
20842|Yardarino Sandstone Member|31910|4|Described|Table 1|||P18||||||
20842|Yardarino Sandstone Member|32642|6|Mentioned|p74|||Oil Production||||||
20842|Yardarino Sandstone Member|36293|6|Mentioned|p111|||See also P123.||||||
20842|Yardarino Sandstone Member|36890|4|Described|p235|||Formerly Yardarino Sandstone||||||
20842|Yardarino Sandstone Member|38484|6|Mentioned|p6|||||||||
20842|Yardarino Sandstone Member|38486|6|Mentioned|p6|||||||||
20842|Yardarino Sandstone Member|41195|6|Mentioned|p322|||||||||
20842|Yardarino Sandstone Member|44144|6|Mentioned|p507 Tb.4-21, p511 Fig.4-147|Early Triassic|Late Permian|Shoreline deposit.||Wagina Sandstone (top of).||||
20847|Yardie Group|24059|5|Briefly described|p132|Tertiary|Tertiary|Geological Province: Barrow Sub-basin.||||||
20847|Yardie Group|30122|6|Mentioned|p50|||||||||
20847|Yardie Group|30821|6|Mentioned|p59|||Stratigraphic sequence||||||
20847|Yardie Group|32750|6|Mentioned|p311|||Refers Condon (1968). Invalid.||||||
20847|Yardie Group|33386|6|Mentioned|Fig.7|||||||||
20847|Yardie Group|33453|6|Mentioned|p72|||Strat.||||||
20847|Yardie Group|35105|6|Mentioned|p83|||||||||
20847|Yardie Group|35282|6|Mentioned|Fig.21|||||||||
20847|Yardie Group|41712|6|Mentioned|Fig.8|||||||||
20847|Yardie Group|44959|6|Mentioned|p.27|||||||||
20847|Yardie Group|45015|5|Briefly described|map legend|Tertiary|Tertiary|Comprises Pilgramunna Formation and Vlaming Sandstone. Age is Late Tertiary.||||||31-MAY-06
20847|Yardie Group|45142|6|Mentioned|p25|||||||||
20847|Yardie Group|46950|6|Mentioned|Fig.15|||||||||
20847|Yardie Group|46983|6|Mentioned|Fig.2|||||||||
20847|Yardie Group|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Includes: Pilgramunna Formation and Vlaming Sandstone.||||||
20871|Yarragadee Formation|12758|4|Described|p18, p3 Fig. 3|Late Jurassic|Middle Jurassic|Redefined by Backhouse (1984). Conformably overlain by Otorowiri Formation; conformably overlies the Cadda Fm. Directly overlies Cattamarra C.M. in the Mandurah Terrace and Bunbury Trough.  Age: ~180-140Ma.  Max. thick: 1510m.  Geol. Prov: Perth Basin.||||||28-JUL-09
20871|Yarragadee Formation|12759|3|Fully described|p27; p28 Tb. 7; p174 Pl. 2|Tithonian|Aalenian|Defined McWhae et al (1958); original type section 2.4 km SSE of Yarragadee Homestead. New ref. section nominated for Gingin No. 1 Well (356 -3315 m): Playford et al. (1976) and Backhouse (1984).|||||Over 2000m of interbedded sandstone, siltstone and shale.|12-MAY-14
20871|Yarragadee Formation|14227|5|Briefly described|p6, p8, p11|Late Jurassic|Late Jurassic|Age is: Bajocian-Tithonian. Geological Province: Hautman Sub-basin. Fluvial deposits. See also Enclosure 2.||||||07-FEB-11
20871|Yarragadee Formation|22769|5|Briefly described|p755||Late Jurassic|Thick fluvial deposits. Max. thickness: 3.6km. Geological Province: Perth Basin.||||||17-JAN-06
20871|Yarragadee Formation|22814|5|Briefly described|fig2|Jurassic|Jurassic|||||||
20871|Yarragadee Formation|22820|6|Mentioned|p23|||Contains valleys eroded into the unit which are lava-filled by Bunbury Basalt. Geological province: southern Perth Basin.||||||12-AUG-08
20871|Yarragadee Formation|23172|4|Described|Map Legend|Jurassic|Jurassic|||||||
20871|Yarragadee Formation|23279|4|Described|p29-30|Tithonian|Bathonian|||||||
20871|Yarragadee Formation|23520|5|Briefly described|p6 Fig. 4|Late Jurassic|Middle Jurassic|Conformably overlies the Cadda Formation.  Geological Province: Abrolhos Sub-basin and Perth Basin.  See also p9 and p16.||||||
20871|Yarragadee Formation|23578|5|Briefly described|p6|Jurassic|Jurassic|||||||
20871|Yarragadee Formation|23579|5|Briefly described|Map Legend|||||||||
20871|Yarragadee Formation|23761|4|Described|p6|Late Jurassic|Late Jurassic|Interbedded sandstone, siltstone and shale. Max. thickness: 2500m. Geological Province: Dandaragan Trough||||||01-OCT-08
20871|Yarragadee Formation|23816|5|Briefly described|p230, 241|Early Cretaceous|Middle Jurassic|Formerly known as the "Yarragadee Beds". Geological Province: Perth Basin. Underlying units: Cadda Formation and Cockleshell Gully Formation (both conformable). Overlying unit: Warnbro Group (unconformable). Max. thickenss: >3000 m. Fossiliferous.||||||27-APR-05
20871|Yarragadee Formation|24020|5|Briefly described|p387|Early Cretaceous|Late Jurassic|Geological Province: Perth Basin||||||16-MAR-05
20871|Yarragadee Formation|24058|5|Briefly described|p112|Late Jurassic|Late Jurassic|Geological Basin: Perth Basin.||||||
20871|Yarragadee Formation|24160|5|Briefly described|p94, p95|Cretaceous|Jurassic|Perth Basin. Source of clay and shale used in the brick industry.||||Is overlain unconformably by Leederville Formation.|Interbedded sandstone and siltstone, with lesser thicknesses of shale, claystone and conglomerate; mottled red, yellow and white colours characteristic.|
20871|Yarragadee Formation|24351|5|Briefly described|Plate 3 (in pocket)|Tithonian|Bajocian|Log Houtman-1. Name written as Yarragadgee only.||||||23-JAN-08
20871|Yarragadee Formation|24374|5|Briefly described|p8|||Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|24390|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|24410|5|Briefly described|p41|Jurassic|Jurassic|Contains appreciable quantities of white quartz sand. Geological Province: northern Perth Basin.||||||24-NOV-09
20871|Yarragadee Formation|24443|5|Briefly described|p25, 31|Late Jurassic|Middle Jurassic|Overlies Cadda Formation. Overlain by Parmelia Group (conformable) and Warnbro Group (unconformable). Geological Province: Vlaming Sub-basin, Houtman Sub-basin.||||||28-JUL-09
20871|Yarragadee Formation|29382|6|Mentioned|Table 10|||||||||
20871|Yarragadee Formation|29602|6|Mentioned|p99|||||||||
20871|Yarragadee Formation|29603|6|Mentioned|p107|||||||||
20871|Yarragadee Formation|29689|5|Briefly described|p106|||||||||
20871|Yarragadee Formation|29693|6|Mentioned|Fig.7|||||||||
20871|Yarragadee Formation|29721|6|Mentioned|Table 226|||||||||
20871|Yarragadee Formation|29790|6|Mentioned|p94|||||||||
20871|Yarragadee Formation|30188|2|Defined|p73|Early Cretaceous|Middle Jurassic|Middle Jurassic to Early Cretaceous||||||
20871|Yarragadee Formation|30628|6|Mentioned|p1958|||Wells abandoned||||||
20871|Yarragadee Formation|30820|6|Mentioned|p47|||||||||
20871|Yarragadee Formation|30948|6|Mentioned|Map legend|Jurassic|Jurassic|Tithonian - Bajocian||||||
20871|Yarragadee Formation|30963|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic to Cretaceous||||||
20871|Yarragadee Formation|31153|6|Mentioned|Fig. 57|||Stratigraphic table. Refers Cockbain & Playford (1973).||||||
20871|Yarragadee Formation|31238|4|Described|p27|||||||||
20871|Yarragadee Formation|31561|5|Briefly described|p18|||See also p20, 24, Section p22.||||||07-OCT-20
20871|Yarragadee Formation|31562|6|Mentioned|p10|||Stratigraphic table||||||
20871|Yarragadee Formation|31568|5|Briefly described|p18|||U. Jurassic||||||
20871|Yarragadee Formation|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
20871|Yarragadee Formation|31859|6|Mentioned|p1063|||||||||
20871|Yarragadee Formation|31899|6|Mentioned|p36|||||||||
20871|Yarragadee Formation|31910|3|Fully described|Table 1|||p22.||||||07-OCT-20
20871|Yarragadee Formation|31912|6|Mentioned|p55|||||||||
20871|Yarragadee Formation|32648|6|Mentioned|p32|||Jur.-Cret.||||||
20871|Yarragadee Formation|32649|4|Described|p26|||See also Table 1||||||
20871|Yarragadee Formation|32714|6|Mentioned|Fig.2|||||||||
20871|Yarragadee Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
20871|Yarragadee Formation|33022|6|Mentioned|p261|||||||||
20871|Yarragadee Formation|33044|6|Mentioned|Fig.16|||Shown on diag.16||||||
20871|Yarragadee Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
20871|Yarragadee Formation|33166|6|Mentioned|Fig.1|||Geological map.||||||
20871|Yarragadee Formation|33386|6|Mentioned|Fig.7|||||||||
20871|Yarragadee Formation|33552|6|Mentioned|p58|||L.Cret. Oil traces||||||
20871|Yarragadee Formation|33747|6|Mentioned|p1072|||||||||
20871|Yarragadee Formation|34112|6|Mentioned|p3|||||||||
20871|Yarragadee Formation|34134|6|Mentioned|Cor.Chart|||Middle - Upper Jurassic.||||||
20871|Yarragadee Formation|34841|6|Mentioned|Fig.2|||||||||
20871|Yarragadee Formation|35058|6|Mentioned|p64|||||||||
20871|Yarragadee Formation|35093|6|Mentioned|p48|||||||||
20871|Yarragadee Formation|35152|6|Mentioned|p3|||||||||
20871|Yarragadee Formation|35282|6|Mentioned|p31|||See also Fig.2.||||||
20871|Yarragadee Formation|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
20871|Yarragadee Formation|35653|6|Mentioned|p1094|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
20871|Yarragadee Formation|35968|6|Mentioned|p60|||Hydrogeology on P65.||||||
20871|Yarragadee Formation|35970|5|Briefly described|p81|||Discussion re hydrogeology.||||||
20871|Yarragadee Formation|35983|6|Mentioned|p148|||||||||
20871|Yarragadee Formation|36100|6|Mentioned|Fig.2|||||||||
20871|Yarragadee Formation|36257|6|Mentioned|Table 2.1|||||||||
20871|Yarragadee Formation|36265|5|Briefly described|Fig.3.26|Late Jurassic|Late Jurassic|Geological province: Perth Basin.||||||04-MAR-08
20871|Yarragadee Formation|36268|5|Briefly described|p175||Early Cretaceous|Contains an aquifer providing pressure water used by processing plants.||||||12-MAR-08
20871|Yarragadee Formation|36293|2|Defined|p157|Neocomian|Middle Jurassic|Middle Jurassic to Neocomian.||||||
20871|Yarragadee Formation|36331|6|Mentioned|p64|||||||||
20871|Yarragadee Formation|36890|3|Fully described|p241|||Formerly Yarragadee Beds. Includes Capel River Gp, Fly Brook Sh. See p230.||||||07-OCT-20
20871|Yarragadee Formation|36911|6|Mentioned|p58|||||||||
20871|Yarragadee Formation|37104|6|Mentioned|Fig.3|||||||||
20871|Yarragadee Formation|37124|6|Mentioned|p339|||||||||
20871|Yarragadee Formation|37286|6|Mentioned|Figure|||On page 30.||||||
20871|Yarragadee Formation|37298|6|Mentioned|Fig.1|||||||||
20871|Yarragadee Formation|37308|5|Briefly described|Table 4|||Hydrogeology p25.||||||07-OCT-20
20871|Yarragadee Formation|37309|4|Described|p16|||Groundwater P18.||||||
20871|Yarragadee Formation|37340|6|Mentioned|p164|||||||||
20871|Yarragadee Formation|37341|6|Mentioned|p230|||||||||
20871|Yarragadee Formation|37499|6|Mentioned|p377|||||||||
20871|Yarragadee Formation|37577|6|Mentioned|p64|||||||||
20871|Yarragadee Formation|38221|6|Mentioned|p353|||||||||
20871|Yarragadee Formation|38479|3|Fully described|p15|||||||||
20871|Yarragadee Formation|38777|3|Fully described|p29|||||||||
20871|Yarragadee Formation|38778|6|Mentioned|Fig.5|||||||||
20871|Yarragadee Formation|39022|6|Mentioned|p397|||||||||
20871|Yarragadee Formation|39155|5|Briefly described|p15|||Aquifer characteristics||||||
20871|Yarragadee Formation|39156|4|Described|p22|||||||||
20871|Yarragadee Formation|39211|6|Mentioned|p61|||See also P63||||||
20871|Yarragadee Formation|39794|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
20871|Yarragadee Formation|39915|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
20871|Yarragadee Formation|40300|1|Redefined|p1|Tithonian|Bathonian|Middle to Late Jurassic. Old Yaragadee Formation of Playford and others, 1976 is revised to pre-Otorowiri Member rocks. Palynomorphs are only frequently recorded fossils.||||Overlain by Otorowiri Member, Parmelia Formation.|Discontinuous medium grey to white, fine to coarse sandstone units and thin shale beds. Carbonaceous stringers common.|07-OCT-20
20871|Yarragadee Formation|40304|3|Fully described|p37|||||||||
20871|Yarragadee Formation|40305|4|Described|p78|||||||||
20871|Yarragadee Formation|40306|6|Mentioned|p59|||||||||
20871|Yarragadee Formation|40346|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
20871|Yarragadee Formation|40347|6|Mentioned|p1|||See also P25||||||
20871|Yarragadee Formation|40348|6|Mentioned|Map legend|Early Cretaceous|Middle Jurassic|Middle Jurassic to Lower Cretaceous||||||
20871|Yarragadee Formation|40349|5|Briefly described|p16|||||||||
20871|Yarragadee Formation|40358|6|Mentioned|p22|||||||||
20871|Yarragadee Formation|40359|5|Briefly described|p22|||||||||
20871|Yarragadee Formation|40367|6|Mentioned|Fig.2 p73|||||||||07-AUG-07
20871|Yarragadee Formation|40395|6|Mentioned|p333|||||||||
20871|Yarragadee Formation|40992|6|Mentioned|Fig.5|||||||||
20871|Yarragadee Formation|41195|6|Mentioned|Fig.2|||||||||
20871|Yarragadee Formation|41271|6|Mentioned|p214|||||||||
20871|Yarragadee Formation|41284|4|Described|p91|||||||||
20871|Yarragadee Formation|41728|6|Mentioned|p441|||See also Fig.3||||||
20871|Yarragadee Formation|41729|5|Briefly described|p454|||||||||
20871|Yarragadee Formation|41781|6|Mentioned|p14|||||||||
20871|Yarragadee Formation|41782|4|Described|p23|||See also p35.||||||07-OCT-20
20871|Yarragadee Formation|41989|4|Described|p110|||||||||
20871|Yarragadee Formation|42075|5|Briefly described|Fig.7 p247|||See also p229.||||||07-OCT-20
20871|Yarragadee Formation|42194|4|Described|p2|||||||||
20871|Yarragadee Formation|42434|4|Described|p5|||||||||
20871|Yarragadee Formation|42687|6|Mentioned|map legend|Jurassic||||||||
20871|Yarragadee Formation|42688|6|Mentioned|map legend|Jurassic||||||||
20871|Yarragadee Formation|42734|5|Briefly described|map legend|Jurassic||||||||
20871|Yarragadee Formation|43031|4|Described|p16,Fig.2.|||||||||
20871|Yarragadee Formation|43062|5|Briefly described|p23,Table 2,p18|||||||||
20871|Yarragadee Formation|43096|4|Described|p5|||see also Fig.2.||||||07-OCT-20
20871|Yarragadee Formation|43189|5|Briefly described|Map Legend||Jurassic|||||||
20871|Yarragadee Formation|43197|5|Briefly described|Map Legend||Jurassic|||||||
20871|Yarragadee Formation|43212|5|Briefly described|p6||Jurassic|||||||
20871|Yarragadee Formation|43216|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
20871|Yarragadee Formation|43217|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
20871|Yarragadee Formation|43252|5|Briefly described|p104|||||||||
20871|Yarragadee Formation|43296|5|Briefly described|Map Legend||Jurassic|||||||
20871|Yarragadee Formation|43297|4|Described|Fig.3 p5, p15.|Late Jurassic|Middle Jurassic|see also table 1 p6. Type section location given.||||||07-OCT-20
20871|Yarragadee Formation|43347|4|Described|5|Late Jurassic|Middle Jurassic|||||||
20871|Yarragadee Formation|43495|4|Described|3-36|Tithonian|Bathonian|||||||
20871|Yarragadee Formation|43504|4|Described|4-11|Berriasian|Bathonian|||||||
20871|Yarragadee Formation|43825|6|Mentioned|p148|||||||||
20871|Yarragadee Formation|44144|4|Described|p505 Tb.4-21, p509 Fig.4-145, p514-515|Tithonian|Middle Jurassic|See also p525 fig 4-170. Type Section: SSE of Yarragadee homestead; 29o05'48''S 115o24'50''E. Reference section in Gingin 1: 356-3315 m. 3000m thick fluvial deposits.||||Overlies Cadda Formation, Cockleshell Gully Formations and Kojarena Sandstone (all conformably). Overlain by Parmelia Formation (conformably), and Bunbury Basalt (unconformably).|Grey to white, fine- to coarse-grained sandstone with thin shale beds.|
20871|Yarragadee Formation|44237|14|Not recorded|p.199,203||Late Jurassic|(U.Jurassic).||||||
20871|Yarragadee Formation|44303|4|Described|p.7,8,9,11,13,19,20|Early Cretaceous|Late Jurassic|Lower Cretaceous-Upper Jurassic. (I/50-5,9).||||||
20871|Yarragadee Formation|44307|14|Not recorded|p11|Early Cretaceous|Middle Jurassic|L/Cret+Middle Jurassic.||||||
20871|Yarragadee Formation|45168|6|Mentioned|p6|||||||||
20871|Yarragadee Formation|48614|4|Described|p5,31,24, Pl.1,2,9|||(H50-5,9).||||||
20871|Yarragadee Formation|48615|4|Described|p.11,13,21|||Fig.4,6. Pl.2,3.  (H50-1).||||||
20871|Yarragadee Formation|49942|5|Briefly described|p39|Jurassic|Jurassic|Geological Province: Perth Basin. Possibly an oil source rock.||||||
20871|Yarragadee Formation|50085|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Northern Perth Basin.||||||11-MAY-04
20871|Yarragadee Formation|50107|5|Briefly described|Map legend|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|50108|5|Briefly described|Map legend|Late Jurassic|Late Jurassic|Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|60376|4|Described|p23, p17 Fig. 4, p 29.|Late Jurassic|Middle Jurassic|Geological Province: Perth Basin. Overlain by Otorowiri Formation. Underlain by Cadda Formation. Consists of interbedded fine- to coarse-grained feldspathic sandstones, siltstones and claystones with minor conglomerates and coal.||||||22-AUG-18
20871|Yarragadee Formation|60384|6|Mentioned|p243 Fig 2a, p261|Late Jurassic|Middle Jurassic|Perth Basin. Source rocks and potential reservoir.||||||
20871|Yarragadee Formation|60386|6|Mentioned|p299, 302|Early Cretaceous|Middle Jurassic|Perth Basin. Non-marine, proximal shelf and deltaic-nearshore-shelf.||||||
20871|Yarragadee Formation|60556|5|Briefly described|p24|Mesozoic||Mesozoic||||||
20871|Yarragadee Formation|61023|5|Briefly described|p20 Fig. 10|Jurassic|Jurassic|Geological Province: Perth Basin.||||||11-APR-08
20871|Yarragadee Formation|61546|6|Mentioned|p385 Fig.5.|Late Jurassic|Middle Jurassic|||||Overlies Cadda Formation.||
20871|Yarragadee Formation|61811|4|Described|p3, pp33-34, p39, pp45-48, pp53-54, p66.|Kimmeridgian|Bathonian|Northern Perth Basin. The type section, a low hill on Yarragadee Station, does not reveal upper or lower contacts; further details in Appendix 1. A reference section is in Bringo rail cutting, c. 24 km east of Geraldton (nominated by Playford et al. in McWhae et al. 1958). Misnamed as Yarragadee Sandstone on p33. Locally intensely bioturbated.||||Overlies Cadda Formation, and Champion Bay Group conformably. Is overlain by Parmelia Group.|Interbedded poorly-sorted sandstone and siltstone, minor shale and conglomerate, mottled red, yellow and white in weathered exposures.|
20871|Yarragadee Formation|63017|5|Briefly described|p892 Fig.1, p893|Late Jurassic|Middle Jurassic|Age: ~160Ma. Conformably overlain by the Parmelia Formation. Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|63018|5|Briefly described|p907 Fig. 1|Late Jurassic|Middle Jurassic|Overlain by Parmelia Formation. Geological Province: Perth Basin.||||||
20871|Yarragadee Formation|64580|4|Described|map legend|Late Jurassic|Middle Jurassic|Fine- to coarse-grained sandstone, thin shale interbeds.||||||09-DEC-08
20871|Yarragadee Formation|64635|5|Briefly described|p4 Fig.3, p16, p23, p27, p28     |Tithonian|Bathonian|Appears also as Yarragadee Sandstone on p16.||||Upper part is laterally equivalent to the upper part of the Cattamarra Coal Measures and the Cadda Formation. Is overlain by Otorowiri Formation (Parmelia Group).|Pebbly sandstone, silty sandstone, siltstone.|
20871|Yarragadee Formation|64769|6|Mentioned|p129|||Overerlain by Bunbury Basalt.||||||06-MAY-09
20871|Yarragadee Formation|65306|5|Briefly described|p20, p21|Late Jurassic|Late Jurassic|Unconformably overlain by Leederville Formation and Bunbury Basalt. Thick, continental succession of mainly weakly-consolidated sandstone. Forms the Yarragadee aquifer, the most widespread aquifer in the Perth Basin.||||||10-SEP-09
20871|Yarragadee Formation|67115|6|Mentioned|p64 Fig. 2|Jurassic|Jurassic|||||Unconformably underlies Gage Formation and South Perth Shale.||
20871|Yarragadee Formation|67135|5|Briefly described|p5 Fig.7, p32, p33 Fig.42, p72.|Jurassic|Jurassic|Perth Basin. Hosts aquifer used for Perth's potable water supply.||||Overlies Cadda Formation. Is overlain by Parmelia Formation.||
20871|Yarragadee Formation|67340|6|Mentioned|p6-8, 25, 50-63|Jurassic|Jurassic|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.||||||
20871|Yarragadee Formation|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Tithonian|Aalenian|See also Ch4 p30 fig 34, Ch5 p26, Ch8 p11.||||Overlies the Cattamarra Coal Measures and the Cadda Formation. Overlain by the Parmelia Group. Unconformably overlain by the Bunbury Basalt and the South Perth Shale.||
20871|Yarragadee Formation|68135|5|Briefly described|p52 fig 2b |Tithonian|Bathonian|Perth Basin. Hosts plant macrofossil assemblages.||||Overlies Champion Bay Group, Cadda Formation. Is overlain by Parmelia Formation.|Pebbly sandstone.|15-SEP-17
20871|Yarragadee Formation|68254|6|Mentioned|p1036 Fig.2, p1037, p1040, p1042, p1043|Jurassic|Jurassic||||||Sandstone.|
20871|Yarragadee Formation|68811|5|Briefly described|p92 fig 52, p97, p98 fig 56|Jurassic|Jurassic|Hosts an aquifer in the Bunbury area. See also p155 app 1, p180 tbl 39, tbl 183 p41.||||Overlies the Cockleshell Gully Formation. Overlain by the Gage Formation, South Perth Shale, Bunbury Basalt and the Superficial Formation. Unconformably overlain by the Leederville Formation.|Interbedded sandstone, siltstone and shale.|15-APR-20
20871|Yarragadee Formation|69029|6|Mentioned|p330,332|Tithonian|Bathonian|Of Perth Basin. Contains oil- and gas-prone source beds with TOC up to 2%.||||Overlain by Parmelia Group. Underlain by Cada Formation.||
20871|Yarragadee Formation|69081|5|Briefly described|p735-41,  Tbs.1-3, Figs.1-4|Late Jurassic|Middle Jurassic|Presented as Yarragadee in figure and in table. Potential target for geothermal projects. Highest porosity (up to 36%), highest mean porosity (16%), maximum permeability values (up to 1400 mD), highest mean permeability value (~ 45 mD), and lowest thermal conductivity (under dry, 2.6 W m-1 K-1; and saturated 4.3 W m-1 K-1) of the four wells analysed. Geol. Prov: Perth Basin||||Overlies Cadda Formation.|Fine- to coarse-grained, poorly sorted feldspathic sandstone succession.|23-JUL-15
20871|Yarragadee Formation|69182|5|Briefly described|p7, Ch2 p3, Ch2 p14|Late Jurassic|Middle Jurassic|Perth Basin. Fluvial and overbank deposits. Ranges from 2000-4000m thick. Possesses good porosity and permeability but its seal unit is thin and discontinuous. See also Ch2 p15, Ch2 p34-p41, Ch2 p46, Ch2 p52-p55, Ch2 p57, Ch2 p60-p63, Ch2 p69, Ch2 p70-p74, Ch2 p85, Ch2 p99, Ch2 p100, Ch2 p103, Ch2 p107.||||Overlies the Cattamara Coal Measures and the Cadda Formation. Unconformably overlain by the Otorowiri Formation and the Parmelia Group.|Coarse grained clastics,sandstones and local claystones.|
20871|Yarragadee Formation|69297|6|Mentioned|p175, p176, p189, p224|Tithonian|Bajocian|Vlaming Sub-basin, Perth Basin. Contains numerous proven intraformational seals.||||Overlies the Cattamarra Coal Measures. Overlain by the Parmelia Group.||
20871|Yarragadee Formation|70097|5|Briefly described|p3, p8, p19-22 Figs.3-6|Tithonian|Bajocian|Perth Basin. Dandaragan Trough, Dongara Saddle, Greenborough/Bookara Shelf, Beermullah Trough, Mandurah Terrace, Vlaming Sub-basin and Bunbury Trough.||||Overlies Cattamarra Coal Measures or Cadda Formation. Is overlain by Otorowiri Formation (Parmelia Group), South Perth Shale (Warnbro Group), or Tamala Limestone.|Fluvial sedimentation. Includes sandstone.|13-SEP-17
20871|Yarragadee Formation|70099|5|Briefly described|Fig.4; p4-5|Tithonian|Bajocian|Vlaming Sub-basin. Correlated to Mentelle 2 and 3 syn-rift Supersequences.||||Overlies Cattamarra Coal Measures. Is overlain by Jervoise Sandstone (Parmelia Group).||
20871|Yarragadee Formation|70128|5|Briefly described|p449, p451, p454-455, p457, p459-464|Late Jurassic|Middle Jurassic|Perth Basin. Modelled thickness distribution histogram.||||Conformably overlies Cadda Formation and Cattamarra Coal Measures. Is overlain conformably by Parmelia Group.||
20871|Yarragadee Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Tithonian|Middle Jurassic|Perth Basin. Formed during Gondwana breakup along the western margin.|174.1  145 Ma (biostrat)||||Fine to coarse-grained sandstone, thin shale interbeds.|07-OCT-20
20871|Yarragadee Formation|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Perth Basin.||||||
20871|Yarragadee Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, conglomerate, sandstone|
20871|Yarragadee Formation|71269|5|Briefly described|GEOL_LUT_CSV files|Tithonian|Middle Jurassic|Of Perth Basin. 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.|174.1-150 Ma (biostrat)||||Fine- to coarse-grained sandstone, thin shale interbeds|
20871|Yarragadee Formation|71377|5|Briefly described|p7|Late Jurassic|Middle Jurassic|Perth Basin.||||||
20871|Yarragadee Formation|71780|14|Not recorded|p50-54, p51 Table 1, Plate 2||Late Jurassic|Sediments in this group now part of South Perth Fm., upper Jurrasic; described on p50.||||||
20871|Yarragadee Formation|71958|5|Briefly described|p6, p14, p33-p34, p41, p47|Late Jurassic|Middle Jurassic|Vlaming Sub-basin, Perth Basin. Primarily composed of fluvio-lacustrine successions. Coals and shales are considered prospective for hydrocarbon generation. Several potential plays are described in Miyazaki et al (1996).||||Overlies the Cattamarra Coal Measures and the Cadda Formation. Overlain by the Parmelia Group.|Coal, carbonaceous shales, feldspathic sandstone and siltstones.|
20871|Yarragadee Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tithonian|Middle Jurassic|Perth Basin.  Age from biostratigraphy.|||||Fine- to coarse-grained sandstone, thin shale interbeds.|
20871|Yarragadee Formation|72258|5|Briefly described|p129|Late Jurassic|Middle Jurassic|Of Perth Basin.||||Underlain by, and laterally grades northward into Cadda Formation. Also underlain by Cattamarra Coal Measures.||15-JAN-20
20871|Yarragadee Formation|73513|5|Briefly described|p30 Fig.2, p33|Berriasian|Bathonian|Perth Basin.||||Overlies Cadda Formation, underlies Parmelia Group|Sandstone.|
20890|Yarrawolya Formation|23569|4|Described|p4 Tb. 1|Proterozoic|Proterozoic|Parent: Badgeradda Group.   Siltstone and silty sandstone, locally hematitic.||||||
20890|Yarrawolya Formation|24114|5|Briefly described|p8|Neoproterozoic|Mesoproterozoic|Of Badgeradda Group. Geological Province: Yilgarn Craton.||||||
20890|Yarrawolya Formation|36199|6|Mentioned|p1|||||||||
20890|Yarrawolya Formation|36293|6|Mentioned|p77|||||||||
20890|Yarrawolya Formation|38494|4|Described|p27|||||||||
20890|Yarrawolya Formation|40336|5|Briefly described|p15|||||||||
20890|Yarrawolya Formation|40339|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
20890|Yarrawolya Formation|43835|5|Briefly described|Map Legend||Proterozoic|||||||
20890|Yarrawolya Formation|44142|5|Briefly described|p328 Tb.4-5|||Mis-spelt as Yarrawalya Formation.||Badgeradda Group|||Siltstone, silty sandstone.|
20890|Yarrawolya Formation|45015|2|Defined|p22-24, map legend||Proterozoic|Top unit of Badgeradda Group. Laminated siltstone and fine-grained quartzwacke. Conformably overlies Coomberarie Formation; unconformably overlain by Lyons Group. Thickness (probably truncated): 1435ft. Geological Province: Carnarvon Basin.||||||31-MAY-06
20890|Yarrawolya Formation|48823|3|Fully described|p3 Tb. 1, p15, map legend|Mesoproterozoic|Mesoproterozoic|Of the Badgeradda Group. Brown to greyish purple, thin bedded, micaceous sandstone, cross-stratified; and brown siltstone. Overlies Coomberarie Fm. Thickness: ~1400ft.  See also p10 Tb. 2.||||||16-JAN-07
20890|Yarrawolya Formation|61958|5|Briefly described|Map sheet 1|Neoproterozoic|Neoproterozoic|Of the Badgeradda Group.||||||21-MAR-06
20890|Yarrawolya Formation|64580|4|Described|map legend||Mesoproterozoic|Of Badgeradda Group. Siltstone and silty sandstone.||||||09-DEC-08
20890|Yarrawolya Formation|69583|5|Briefly described|Plate 3|||Badgeradda Basin.||Badgeradda Group.|||Siltstone and silty sandstone.|
20890|Yarrawolya Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
20890|Yarrawolya Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Badgeradda Basin.||Badgeradda Group|||Siltstone and silty sandstone.|
20933|Yellow Drum Formation|23722|5|Briefly described|p34|Early Carboniferous|Late Devonian|Parent: Fairfield Group. Geological Province: Canning Basin.||||||24-NOV-08
20933|Yellow Drum Formation|24390|5|Briefly described|p8|Carboniferous|Devonian|Geological Province: Canning Basin. Of the Fairfield Group.||||||11-APR-08
20933|Yellow Drum Formation|41217|4|Described|p310|||Originally Yellow Drum Sandstone.||||||24-NOV-08
20933|Yellow Drum Formation|41730|6|Mentioned|p485|||||||||
20933|Yellow Drum Formation|42030|5|Briefly described|p747|||||||||
20933|Yellow Drum Formation|42032|6|Mentioned|p513|||||||||
20933|Yellow Drum Formation|42547|6|Mentioned|Fig.41 P115|||||||||
20933|Yellow Drum Formation|42814|6|Mentioned|p23|||Of Fairfield Group.||||||11-APR-08
20933|Yellow Drum Formation|42860|5|Briefly described|Fig.2|||||||||
20933|Yellow Drum Formation|42933|5|Briefly described|Fig.94 p258|||||||||
20933|Yellow Drum Formation|43173|6|Mentioned|54||Early Permian|||||||
20933|Yellow Drum Formation|43666|6|Mentioned|p24||Early Carboniferous|||||||
20933|Yellow Drum Formation|45143|6|Mentioned|Fig.4|||Geology of the Fairfield Group.||||||
20933|Yellow Drum Formation|50085|5|Briefly described|p8|Devonian|Devonian|Of the Fairfield Group. Geological Province: Canning Basin.||||||05-SEP-08
20933|Yellow Drum Formation|61023|5|Briefly described|p12|Carboniferous|Devonian|Of the Fairfield Formation.||||||11-APR-08
20933|Yellow Drum Formation|61551|6|Mentioned|p359, p361.|Late Devonian|Late Devonian|Canning Basin. Hydrocarbon (oil) source in the Blina field.||Unit in the Fairfield Group.||||10-FEB-20
20933|Yellow Drum Formation|64187|5|Briefly described|p320 Fig. 2|Famennian|Famennian|Formation is Fm. in text. Underlain by Gumhole Formation, overlain unconformably by Laurel Formation. Sandstone, dolomite, siltstone (shallow marine). Geological Province: Canning Basin.||||||08-FEB-10
20933|Yellow Drum Formation|64643|5|Briefly described|p3 Fig. 2|Mississippian|Mississippian|||||||09-FEB-18
20933|Yellow Drum Formation|64694|6|Mentioned|p233|Late Devonian|Late Devonian|A negative shift of carbonate carbon and oxygen isotope values in this unit marks the Yellow Drum regression in the Canning Basin, recognised as the Hangenberg Event.||||||
20933|Yellow Drum Formation|64981|5|Briefly described|p667, p670, p672.|Early Carboniferous|Early Carboniferous|Lennard Shelf. Oil recovered from a 10 m thick dolomite interval in this unit in 1981; sourced from Gogo Formation.||Unit in Fairfield Group.||Overlies Gumhole Formation. Is overlain by Laurel Formation.|Carbonates.|
20933|Yellow Drum Formation|65301|5|Briefly described|p5 Fig. 4|Mississippian|Mississippian|Of Fairfield Group. Geological province: Canning Basin.||||||
20933|Yellow Drum Formation|65449|6|Mentioned|p6|Early Carboniferous|Early Carboniferous|||Fairfield Group.||||
20933|Yellow Drum Formation|67131|6|Mentioned|p2, p5|Tournaisian|Famennian|Interchangeable with Yellow Drum Sandstone  p3 Fig. 2 (Playford et al, 2009).||Fairfield Group|||Sandstone.|29-JAN-20
20933|Yellow Drum Formation|68902|5|Briefly described|p9 fig 5|Carboniferous|Carboniferous|||Fairfield Group||Overlies Gumhole Formation; overlain by Laurel Formation.||
20933|Yellow Drum Formation|69182|6|Mentioned|Ch4 p9, Ch4 p13-p14|Tournaisian|Famennian|North Canning Basin. See also Ch4 p38, Ch4 p42, Ch4 p44, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p63, Ch4 p74-p78, Ch4 p84, Ch4 p86, Ch4 p88, Ch4 p90.||Fairfield Group||Overlies the Gumhole Formation. Overlain by the Laurel Formation.||
20933|Yellow Drum Formation|69312|5|Briefly described|p3, p9, p19, p23 fig 27, p26 fig 33|Tournaisian|Famennian|Canning Basin. Reservoir of the Blina crude oil.||Fairfield Group||Overlies the Gumhole Formation. Overlain by the Laurel Formation.|Carbonate shales, marl.|
20933|Yellow Drum Formation|70492|5|Briefly described|p166, 178, 180-181|Early Carboniferous|Early Carboniferous|Canning Basin. Sequence (stratigraphy) development diagram.||Fairfield Group.||Overlies Gumhole Formation. Is overlain by Laurel Formation.|Dolostone, calcareous sandstone and dolomitic siltstone with minor limestone.|
20933|Yellow Drum Formation|70774|5|Briefly described|p4|Mississippian|Late Devonian|Fitzroy Trough and Lennard Shelf, Canning Basin.||Fairfield Group||Overlies the Gumhole Formation. Overlain by the Laurel Formation.||10-FEB-20
20933|Yellow Drum Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Fairfield Group.|||Shallow-marine medium to coarse cross bedded sandstone, porous medium to thickly bedded dolomite brecciated near base, minor shale and siltstone, rare thin limestone beds|
20933|Yellow Drum Formation|71894|5|Briefly described|p4|Tournaisian|Famennian|Canning Basin.||Fairfield Group||Overlies the Gumhole Formation. Overlain by the Laurel Formation.|Sandstone.|
20933|Yellow Drum Formation|72499|5|Briefly described|p7 Fig.6.|Tournaisian|Fammennian|Located in the Fitzroy Trough.||Fairfield Group||Overlies Gumhole Formation and underlies Laurel Formation.|Includes sandstone.|
20933|Yellow Drum Formation|72502|5|Briefly described|p3-5|Tournaisian|Famennian|[Unclear distinction from Yellow Drum Sandstone; appears both terms are used concurrently]. Devonian-Carboniferous boundary tentatively identified in many petroleum wells.||Fairfield Group||Underlain by Gumhole Formation.|Consists of a series of massive calcareous sandstone and carbonate beds, with minor mudstone, breccia and evaporitic facies.|
20933|Yellow Drum Formation|73117|5|Briefly described|p3|Tournaisian|Famennian|Canning Basin.||Fairfield Group||Underlain[?] by Gumhole Formation. Overlain[?] by Laurel Formation.|Dominantly sandstone.|
20935|Yellow Drum Sandstone|22741|5|Briefly described|P24, P25, Table3 P15|Early Carboniferous|Late Devonian|||||||
20935|Yellow Drum Sandstone|22776|4|Described|Table.3|Early Carboniferous|Late Devonian|Parent: Fairfield Group. Fossil assemblage includes brachiopods, gastropods, ostracods and algae.||||||
20935|Yellow Drum Sandstone|23766|5|Briefly described|p15|Early Carboniferous|Late Devonian|Parent: Fairfield Group||||||
20935|Yellow Drum Sandstone|36224|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of the Fairfield Group.  Calcareous sandstone; medium to coarse dolomite; minor shale, siltstone, limestone.  Late Devonian to Early Carboniferous.||||||01-FEB-05
20935|Yellow Drum Sandstone|36225|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
20935|Yellow Drum Sandstone|38277|6|Mentioned|p154|||||||||
20935|Yellow Drum Sandstone|39702|6|Mentioned|p225|||||||||
20935|Yellow Drum Sandstone|40866|6|Mentioned|p181|||||||||
20935|Yellow Drum Sandstone|41023|4|Described|p288|||||||||
20935|Yellow Drum Sandstone|41215|6|Mentioned|p278|||||||||
20935|Yellow Drum Sandstone|41217|6|Mentioned|p310|||||||||
20935|Yellow Drum Sandstone|41283|6|Mentioned|p79|||||||||
20935|Yellow Drum Sandstone|41839|3|Fully described|p21|||||||||
20935|Yellow Drum Sandstone|42032|6|Mentioned|p513|||||||||
20935|Yellow Drum Sandstone|42347|6|Mentioned|Fig.2 P1020|||||||||
20935|Yellow Drum Sandstone|42547|4|Described|p92|||||||||
20935|Yellow Drum Sandstone|42811|5|Briefly described|p43|||of Fairfield Group||||||
20935|Yellow Drum Sandstone|42880|5|Briefly described|Fig.2,p1020|||||||||
20935|Yellow Drum Sandstone|43563|6|Mentioned|Fig.5,p10|Early Carboniferous|Late Devonian|||||||
20935|Yellow Drum Sandstone|43818|6|Mentioned|Table 2,p42|||||||||
20935|Yellow Drum Sandstone|44143|4|Described|p.437 Table 4-19|Early Carboniferous|Late Devonian|Unit in Fairfield Group. Up to 350m thick; sandstone and dolomite; shallow marine. Conformable on Gumhole Formation; is overlain conformably by Laurel Formation. Type section is a low ridge 1km NE of Yellow Drum Bore (NOONKANBAH: 18deg 07' 35" S, 125deg 27' 25" E).||||||24-NOV-17
20935|Yellow Drum Sandstone|45133|4|Described|p2|||||||||
20935|Yellow Drum Sandstone|45143|2|Defined|p17|Tournaisian|Tournaisian|||||||
20935|Yellow Drum Sandstone|45153|2|Defined|App.3-56|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
20935|Yellow Drum Sandstone|45158|4|Described|p22|||||||||
20935|Yellow Drum Sandstone|45169|6|Mentioned|p13|||||||||
20935|Yellow Drum Sandstone|46794|5|Briefly described|p64|||Ref. Druce & Radke||||||
20935|Yellow Drum Sandstone|48978|4|Described|p4|||Geochemistry P13 etc.||||||
20935|Yellow Drum Sandstone|64580|6|Mentioned|map legend|||Of Fairfield Group.||||||15-DEC-08
20935|Yellow Drum Sandstone|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
20935|Yellow Drum Sandstone|66127|5|Briefly described|p442-443, Plates 2, 7.|Tournaisian|Famennian|Its lower part contains a miospore assemblage including Retispora lepidophyta, a well-documented marker of the Devonian-Carboniferous boundary.||Unit in the upper part of the Fairfield Group.||Overlies Gumhole Formation. Is overlain by Laurel Formation.|Fluvial to paralic sandstone and dolomite; minor shale and siltstone.|
20935|Yellow Drum Sandstone|67131|6|Mentioned|p3 Fig. 2|Tournaisian|Famennian|Interchangeable with Yellow Drum Formation (p2, p5) (Copp, 2011).||Fairfield Group|||Sandstone.|29-JAN-20
20935|Yellow Drum Sandstone|68298|5|Briefly described|p234|Famennian|Famennian|Canning Basin. Antiarchs (indeterminate) in latest Famennian.||||||
20935|Yellow Drum Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Famennian|||Fairfield Group||||
20935|Yellow Drum Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Famennian|||||||
20935|Yellow Drum Sandstone|69297|6|Mentioned|p337, p352, p356|Tournaisian|Tournaisian|Broome Platform of the Canning Basin. Mistakenly referred to as the Yellow Drum Formation on p356.||Fairfield Group||Overlies the Gumhole Formation. Overlain by the Laurel Formation.||
20935|Yellow Drum Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Fairfield Group.||||
20935|Yellow Drum Sandstone|71267|5|Briefly described|Lithstrat.csv|Tournaisian|Famennian|Files in Explanatory Notes folder. Age given as 362 - 346.7 Ma.|||||Sandstone, lesser dolomite|
20935|Yellow Drum Sandstone|72502|6|Mentioned|p4|||[Unclear distinction from Yellow Drum Formation; appears both terms are used concurrently]. Devonian-Carboniferous boundary placed at 7.5 m above the base of the unit based on the first appearance of the conodont Siphonodella sulcata.||||||
20942|Yelma Formation|7161|5|Briefly described|p90, p99 Fig.9, p100, 101|Statherian|Statherian|Earaheedy Basin. Age is set by K-Ar diagenetic glauconite within this formation. Approximately 1600m thick (from p99 Fig.9).|1698 +/- 12 Ma|||||08-APR-13
20942|Yelma Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Earaheedy Basin.||Of the Tooloo Subgroup.||Is overlain by Frere Formation.|Quartz arenite and shale with a few lenses of stromatolitic carbonate towards the top.|
20942|Yelma Formation|12099|5|Briefly described|p686|Paleoproterozoic|Paleoproterozoic|||Unit in Earaheedy Group.||Unconformably overlies Juderina Formation.||04-MAR-13
20942|Yelma Formation|22478|6|Mentioned|p23||Paleoproterozoic|Earaheedy Group, Nabberu Basin||||||07-NOV-08
20942|Yelma Formation|22493|6|Mentioned|p90|Statherian|Orosirian|1698+/-12Ma||||||
20942|Yelma Formation|22501|6|Mentioned|p117 Fig.3|||in the Earaheedy Basin||||||
20942|Yelma Formation|22716|6|Mentioned|p236|Mesoproterozoic|Mesoproterozoic|||||||
20942|Yelma Formation|23133|5|Briefly described|p293 Fig.1|||Of Earaheedy Basin.||||||28-JUL-08
20942|Yelma Formation|23151|5|Briefly described|p67|||of Yerrida Basin.||||||
20942|Yelma Formation|23529|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Parent: Toodoo Subgroup.  Thickness: ~<1000m.  Geological Province: Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup, Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group, Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|23580|5|Briefly described|Map legend||Proterozoic|Of the Earaheedy Group in the Earaheedy Basin||||||
20942|Yelma Formation|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Earaheedy Group in the Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|23587|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|23588|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Overlying unit Frere Formation. Geological Province: Earaheedy Basin. Max. thickness: 50 m.||||||07-NOV-08
20942|Yelma Formation|23589|4|Described|p20|Calymmian|Statherian|1700 Ma (K-Ar (glauconite)), 1590-1710 (Rb-Sr (glauconite)). Of Tooloo Subgroup. Overlying unit Frere Formation. Underlying unit Yerrida Group. Earaheedy Basin. Max. thickness: 1500 m.||||||
20942|Yelma Formation|23597|4|Described|p11|||Of Earaheedy Group. Max. thickness: ~1600 m.||||||
20942|Yelma Formation|23600|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Age: 2008+/-68 Ma, 1946+/-11 Ma. Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1.  Of Tooloo Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|23747|6|Mentioned|p4|||||||||
20942|Yelma Formation|23749|5|Briefly described|p14|Proterozoic|Proterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
20942|Yelma Formation|23865|6|Mentioned|p173 Fig.2|||Of Earaheedy Group. Geological Province: Yilgarn Craton.||||||
20942|Yelma Formation|23890|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup.  Age: 1946+/-71Ma; 2008+/-68Ma.  See also p21 Fig. 11.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|24017|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|24021|4|Described|p17|Paleoproterozoic|Paleoproterozoic|Parent: Tooloo Subgroup. Geological Province: Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup, Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|24578|4|Described|p776 Fig.1, p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Overlain by the Frere Formation. Age: ~1900 Ma. Geological Province: Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|30010|6|Mentioned|p45|||||||||
20942|Yelma Formation|31217|2|Defined|p40|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
20942|Yelma Formation|36551|6|Mentioned|Table 29|||||||||
20942|Yelma Formation|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|37300|6|Mentioned|p81|||||||||
20942|Yelma Formation|37460|3|Fully described|p137|||||||||
20942|Yelma Formation|38515|4|Described|p9|||||||||
20942|Yelma Formation|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|38978|3|Fully described|p148|||||||||
20942|Yelma Formation|38994|6|Mentioned|p34|||||||||
20942|Yelma Formation|39894|5|Briefly described|p48|||Age dates||||||
20942|Yelma Formation|40103|6|Mentioned|Table 1|||||||||
20942|Yelma Formation|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|40355|4|Described|p5|||||||||
20942|Yelma Formation|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|40938|2|Defined|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20942|Yelma Formation|40939|5|Briefly described|p106|||||||||
20942|Yelma Formation|40989|4|Described|p30|||||||||
20942|Yelma Formation|41997|6|Mentioned|p73|||||||||
20942|Yelma Formation|43069|5|Briefly described|p19|||||||||
20942|Yelma Formation|43238|5|Briefly described|p7|||Earaheedy Group||||||
20942|Yelma Formation|43595|5|Briefly described|p344,Fig.3-42,p345|||||||||
20942|Yelma Formation|43652|6|Mentioned|p381|||||||||
20942|Yelma Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Earaheedy Group.  Quartz arenite, stromatolitic dolomite and associated chert breccia.||||||18-MAY-04
20942|Yelma Formation|44830|5|Briefly described|Map Legend||Proterozoic|||||||
20942|Yelma Formation|49893|5|Briefly described|p5|Proterozoic|Proterozoic|Of the Earaheedy Group. Overlies the Yerrida Group. Age: 1946+/-71 Ma and 2008+/-68 Ma.||||||
20942|Yelma Formation|50008|5|Briefly described|p48|||Age of zircon populations given. Geological Province: Earaheedy Basin.||||||
20942|Yelma Formation|50188|5|Briefly described|p2 Fig. 1, p4 Fig. 2|||Of the Tooloo Subgroup (Earaheedy Group). Contains the Yadgimurrin Member. Geological Province: Earaheedy basin.  Maximum Thickness: 1600m.||||||16-JUL-08
20942|Yelma Formation|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup. Includes the Sweetwaters Well Member and Yadgimurrin Member.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|50222|4|Described|p320 Fig. 3, p328|Paleoproterozoic|Paleoproterozoic|Base of the Tooloo Subgroup (Earaheedy Group).  Includes the Sweetwaters Well Member.  Shale, sandstone and carbonate.  Max. thickness: 500m.  Geological Province: Earaheedy Basin.  See also p319 Fig. 2.||||||07-NOV-08
20942|Yelma Formation|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group).  Shale, sandstone, carbonate. Age: ~1850Ma (Grey, 1994); also, 1770-1740Ma (galena, Pb-Pb: Teen, 1996).  Max. thickness: >500m.  Geological Province: Earaheedy Basin.  See also p351-354.||||||07-NOV-08
20942|Yelma Formation|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Quartz arenite; shale, stromatolitic carbonate, chert, conglomerate. Includes Sweetwaters Well and Yadgimurrin members. Unconformably overlies Yerrida Group. Geol Prov: Earaheedy Basin.||||||07-FEB-11
20942|Yelma Formation|50226|5|Briefly described|p423, p424 Fig. 5|||Basal part of the Tooloo Subgroup (Earaheedy Group).  Sandstone and stromatolitic carbonates.  Overlain by the Frere Formation; unconformably overlies Windplain Group (Yerrida Basin).  Geological Province: Earaheedy Basin.||||||
20942|Yelma Formation|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin. Of the Tooloo Subgroup (Earaheedy Group).  Underlies: Frere Formation.||||||07-NOV-08
20942|Yelma Formation|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Sandstone, siltstone, and phyllitic shale; shallow marine to fluvial deposits.||||||07-NOV-08
20942|Yelma Formation|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin||||||07-NOV-08
20942|Yelma Formation|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Overlain by Frere Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Quartz sandstone, siltstone, shale, and associated chert breccia.  Geological Province: Earaheedy Basin.||||||07-NOV-08
20942|Yelma Formation|61560|6|Mentioned|p491|Archean|Archean|Max. depositional age: 2027+/-23Ma (Pirajno et al 2003).||||||07-NOV-08
20942|Yelma Formation|61564|5|Briefly described|p589, p591|||Of the Earaheedy Group. Includes the Sweetwater Well Member and cross-bedded sandstone.||||||
20942|Yelma Formation|62289|4|Described|plate 1, p6, p29-32, Fig. 29|Palaeoproterozoic|Palaeoproterozoic|Basal unit of Earaheedy Group; includes Sweetwaters Well Member; unconformably overlies Finlayson Member (Juderina Formation, Yerrida Group); age: 1.9-1.8 Ga (Grey 1994); conglomerate, cross-stratified sandstone, chert breccia from stromatolitic dolomite, stromatolitic dolomite, laminated dolomite, dolomitic siltstone, and shale; Geol. Prov: Earaheedy Basin.||||||
20942|Yelma Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Earaheedy Basin.||Of Earaheedy Group.|||Laminated dolomitic siltstone and shale; minor dolomite lenses, stromatolites, and chert bands.|14-APR-11
20942|Yelma Formation|63866|4|Described|p165-p167|Orosirian|Orosirian|Ages are Pb-Pb whole rock dates derived from Russell et al, 1994.May be equivalent to the Mount Leake Formation. Stromatolites suggest ages of 1900 to 1800 Ma (Grey, 1994). Hosts epigenetic Mississippi Valley-type mineralisation.|2008 +/- 68 Ma and 1946 +/- 71 Ma|Tooloo Subgroup|Includes the Sweetwaters Well Member and the Wandiwarra Member.|Overlain by the Frere Formation.||
20942|Yelma Formation|64161|5|Briefly described|p592-593|Statherian|Statherian|Sandstone-rich unit. Unconformably overlies Yilgarn Craton and Yerrida Basin. Ar-Ar dating on mica yields a plateau age of 1658 +/- 1.4 Ma.||Base of Earaheedy Group.||||21-MAR-12
20942|Yelma Formation|64284|4|Described|p58 Fig. 1, p59|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgp(Earaheedy Gp). Incl:Yadgimurrin+Sweetwaters Well Mbrs. Max.thickness: 500m. Geol.prov:Earaheedy Basin. Shale,sandstone+carbonate in shallow marine/locally fluvial deposits; marine transgression at top deposited widespread shale+minor sst.||||||07-FEB-11
20942|Yelma Formation|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Max. thickness: ~1500m. Geological Province: Earaheedy Basin.Sandstone and stromatolitic dolomite.||||||07-FEB-11
20942|Yelma Formation|64580|4|Described|map legend||Paleoproterozoic|Of Tooloo Subgroup. Sandstone, dolomite (locally stromatolitic), siltstone, and shale; minor conglomerate and limestone.||||||09-DEC-08
20942|Yelma Formation|64655|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Sandstone, siltstone, and phyllitic shale; shallow marine to fluvial deposits.||||||
20942|Yelma Formation|64725|5|Briefly described|p59, p73.|Paleoproterozoic|Paleoproterozoic|Host to Magellan Pb deposit.||Basal unit in Tooloo Subgroup.||Unconformably overlies Windplain Group. Is overlain by Frere Formation.|Sandstone and silicified stromatolitic dolomite; silicic and sericitic alteration.|03-APR-12
20942|Yelma Formation|64772|5|Briefly described|p8-9,  Plate 1,  p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Conformable below Frere Fm. Max. dep'l age: 2.03Ga. Geol.prov: Earaheedy Basin. Deeply weathered rocks overlie granites  of Malmac Inlier; shale, sst. and carbonate record a marine transgression.Basal unit of Earaheedy Group. Unconformable over either Archaean basements rocks of granite-greenstone terrane (Yilgarn Craton) or, farther west, with Palaeoproterozoic rocks of Mooloogool Group. Affected by Shoemaker impact structure. See also p17, p18 Fig.8, p20-21 (incl Fig. 10), p23 Tb.2, p25 Fig.11, p25 Fig.12, p26 Fig.13, p27 Fig.15, p28 Fig.16, p32, p32 Fig.20, p33, p33 Fig.21, p36-37, p40 Fig.27, p45, p46, p49-51, p70-71 App.4 Tb.4.2, p72-74 Fig.4.1, p76-77 Fig.4.2, p78 App.4 Tb.4.4, p79-81 App.4 Fig.4.3.||Basal unit of  Tooloo Subgroup (Earaheedy Group)|Includes Sweetwaters Well Member, Yadgimurrin Member|Faulted unconformity beneath Scorpion Group||25-NOV-13
20942|Yelma Formation|64777|6|Mentioned|p6|||Earaheedy Basin. Detrital zircons aged 2500 Ma are rare in WA and known only in this unit, northern Gascoyne Complex and Albany-Fraser Orogen.||||||
20942|Yelma Formation|65264|5|Briefly described|p27, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Conformably overlain by Frere Fm. Geological province: Earaheedy Basin. Comprises pebbly sandstone, arkose, shale, sailtstone, conglomerate, stromatolitic dolomite and minor chert breccia.||||||07-FEB-11
20942|Yelma Formation|65419|1|Redefined|p16, p28, pp46-48, p50.|Paleoproterozoic|Paleoproterozoic|Of Hall et al. (1977); revised by Bunting (1986); Gee and Grey (1993) informally extended the unit to include outliers on Peak Hill and Glengarry 1:250 000 sheets: that assignment is confirmed and formalised in this study. Includes strata previously referred to as the Malmac Formation by Horwitz (1976). Named after Yelma outcamp; the type section is 6 km NW of there. Thickness in this study area is a few tens of metres; up to 1500 m along the northern margin of the Earaheedy Basin. A second age is of 1946 +/- 71 Ma; both from stromatolitic carbonates. Richards and Gee (1985) obtained an age of c.1.7 Ga from galena; that may be mineralization age, not deposition. Coeval with Mount Leake Formation.|2008 +/- 68 Ma (Pb-Pb age; Russell et al. 1994).|Unit in Earaheedy Group.||Unconformably overlies Bubble Well Member (Juderina Formation) and Maraloou Formation, as well as Troy Creek beds. Is overlain conformably by the Frere Formation.|Mature, medium- to coarse-grained quartz arenite; shale; abundant microbial and stromatolitic carbonate, much of which is silicified to a cream, pale-green or grey chalcedonic chert breccia; local basal conglomerate.|
20942|Yelma Formation|65472|5|Briefly described|p4-6, p3 Fig.2, p5 Fig.4, p7 Fig.5|||Thickness range: 3 m in SE to max 1500 m in the Stanley Fold Belt (possible structural repetition in fold belt). Representative 400 m thick section. Age: U-Pb dating of monazite (from peperite margins of interfingering Maraloou Formation and Killara Formation) (Rasmussen and Fletcher, 2002); considered a minimum depositional age for Maraloou Formation and, by inference, provides a maximum age limit for deposition of overlying Yelma Formation. Detrital zircon populations (2.6-2.7 Ga, c.2.2 Ga, c2.0 Ga). Other ages/methods in Fig.2, after Pirajno et al. Deposited in fluvial to coastal setting, with carbonates of the Sweetwaters Well Member developing in saline coastal-lagoonal environment. Earaheedy Basin. Also shown on p8 Figs.6 and 7, p9 Fig.8, p10 (incl.Fig.10), p16, p17 Fig.15a.|c. 1.84 Ga|at base of Tooloo Subgroup (basal unit of Earaheedy Group)|Sweetwaters Well Member|Is overlain by Frere Formation. Disconformably overlies Maralou Formation.|Marine transgressive section of sandstone, shale, carbonate, and minor siltstone and conglomerate.  Includes 100m thick stromatolitic carbonate facies (Sweetwaters Well Member).|25-SEP-15
20942|Yelma Formation|65692|4|Described|p1,p9,p11,p18-25, p28-30, p34-35, p54-56|||See also p59-63, p65-66, p71-75, p79-80. Earaheedy Basin; basal unit. c.1500m thick (on p10 it is given as 3m in the SE to 500m in the NW). Fluvial coastal, and highly saline coastal lagoon, settings. Shows structural repetition, possibly related to deformation during formation of the Stanley Fold Belt. U-Pb-Th and Hf data detailed. Maximum depositional age from detrital zircons (this study).|1971 +/- 26 Ma (Matonia, 2009).|Tooloo Subgroup.|Yadgimurrin, Sweetwaters Well Members.|Is overlain by Frere Formation.|Includes quartz sandstone, siltstone and shale, and stromatolitic dolomite.|
20942|Yelma Formation|65899|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Includes Sweetwaters Well Member and unnamed sandstone unit. Sandstone, dolomite (locally stromatolitic), siltstone and shale; minor conglomerate and limestone.||||||
20942|Yelma Formation|65913|3|Fully described|p3 Table 1, p5, pp19-21.|Paleoproterozoic|Paleoproterozoic|Forms an irregular veneer in small outliers and on top of small mesas. Its base is similar to the Finlayson Member of the Yerrida Group, but has coarser grain size, thicker bedding, weaker cementation, and abundance of trough cross-bedding. Probably tidal to supratidal depositional environment in a broad transgressional event. The stromatolite section has diagnostic taxa including Yandilla meekatharrensis and Yelma digitata. Hosts the Magellan lead-carbonate  mineralization in MEREWETHER sheet.|2008 +/- 68 Ma (Russell et al. 1994).|Basal unit in Earaheedy Group.||Unconformably overlies the Maraloou Formation.|Basal sequence of mature stratified quartz-pebble conglomerate and cross-stratified sandstone; micritic and stromatolitic dolomite intercalated with laminated calcareous arenite and argillite and micritic dolostone; bands of chert and chert breccia.|
20942|Yelma Formation|66427|5|Briefly described|p42-43,p44 Tb.2, p46 Fig.4, p47-55      |||See also p62-63, p71-75. Redefined here to include two Members. Carbonate rocks hosts MVT mineralisation. Several ages from different methods. Mineralisation (Pb) ages mostly cluster around 1650-1700 Ma.||Of the Tooloo Subgroup. |Includes Yadgimurrin and Sweetwaters Well Members.|Unconformably overlies Finlayson Member (Juderina Formation). Possible correlative of the Mount Leake Formation.|Contains sandstone, shale, carbonate and minor siltstone and conglomerate.|
20942|Yelma Formation|67269|5|Briefly described|p20-21 Fig.19|Statherian|Orosirian|Earaheedy Basin. Contains Ephyaltes edingunnensis 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).|2027 +/- 23 to 1698 +/- 12 Ma.|||||
20942|Yelma Formation|67855|5|Briefly described|p207, p208 fig 3-8, p208, 209|Paleoproterozoic|Paleoproterozoic|Up to 1500m thick in Nth, 150m in Sth. 3 facies indicate progressive shallowing NE to SW.||Tooloo Subgroup|||Nth: Alternate feldspathic, micaceous, x-bedded qtz sst, siltstone + shale. Sth: glauconitic + feldspathic qtz sandstone; shale, carbonate overlying. West: thick coarse extensive chert-breccia beds interbedded w stromatolitic dolomite & qtz Sst.|
20942|Yelma Formation|68055|4|Described|p75-80, 84, 87-88|Proterozoic|Proterozoic|Basal unit in the Earaheedy Basin. Possible outliers occur up to 200km S of the main Basin. Sediment was sourced from underlying granitic rocks and/or Mooloogool Group. Geochemistry detailed. Contains authigenic monazite dated at 1811 +/- 13 Ma; a firm minimum age for the unit. Detrital zircons aged ~2.0 Ga (Nelson, 1997) give an MDA.|1815 +/- 13 Ma (SHRIMP U-Pb monazite).|Tooloo Subgroup.|Sweetwaters Well Member.|Overlies Maraloou Formation. Is overlain gradationally by the Frere Formation.|Predominantly sandstones (quartz arenite, glauconitic sandstone, arkose and lithic sandstone), with a complex association of siltstone, shale, carbonate, chert breccia and minor conglomerate.|
20942|Yelma Formation|69003|5|Briefly described|p13 Fig.17, p14-15|||Earaheedy Basin. 10-1500m thick. Sediment derived mainly from the Gascoyne province to the W. Hosts important Pb deposits at Magellan. Age from magmatic zircons from tuffaceous layers.|1970-1950 Ma (SHRIMP U-Pb).|Tooloo Group.|Sweetwaters Well Member.|||
20942|Yelma Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Tooloo Subgroup|Includes Sweetwaters Well Member and 1 unnamed member.||Sandstone, dolomite (locally stromatolitic), siltstone, and shale; minor conglomerate and limestone; fine- to medium-grained sandstone with pebble lags towards base.|07-AUG-15
20942|Yelma Formation|69313|5|Briefly described|p18, p22 Fig.4.2, p23, p25,  p51|Statherian|Orosirian|See also p55, p57, p88, p101, p115, p121, p123.|c. 1810 Ma (Pb-Pb monazite, Muhling et al. 2011)|Tooloo Subgroup|Yadgimurrin Member, Sweetwaters Well Member.|Unconformably (or disconformably) overlain by the Frere Formation|Conglomerate, sandstone, siltstone and limestone.|15-AUG-18
20942|Yelma Formation|69596|5|Briefly described|p10-11|||Earaheedy Basin.||Tooloo Group.|Sweetwaters Well Member.||Interbedded sandstones and siltstones.|
20942|Yelma Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|2027 +/- 23 Ma - 1811 +/- 13 Ma (isotopic).|Tooloo Group|Includes Sweetwaters Well Member||Sandstone, dolomite (locally stromatolitic), siltstone, and shale; minor conglomerate and limestone.|
20942|Yelma Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2027-1811 Ma||||Sandstone, dolomite (locally stromatolitic), siltstone, shale; minor conglomerate and limestone.|
20942|Yelma Formation|71158|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|1971-1949 Ma.|Tooloo Group.|||Sandstone, siltstone and shale; minor conglomerate and dolomite (locally stromatolitic).|
20942|Yelma Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, siltstone, shale, sandstone|
20942|Yelma 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, 100k_geologyp14_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop_lut.csv.|2027+\-23 Ma; 1811+\-13 Ma|Unit of Tooloo Subgroup.|Includes Sweetwaters Well Member, Yadgimurrin Member.||Sandstone; fine- to medium-grained, pebble lags toward base; dolomite (locally stromatolitic) rock, siltstone, and shale; minor conglomerate and limestone.|
20942|Yelma Formation|71484|4|Described|p122,124-125,130-132,135|||Geological province: Of Earaheedy Basin. Thickness: 100m in eastern part of the basin, 300m to central-south, up to 1000m in the NW. Authigenic monazite dated at c. 1815 Ma (Muhling et al., 2012) likely reflects basin deformation rather than local mineralisation (Sheppard et al., 2016).||Unit of Tooloo Group.|Includes Imbin Porphyry.|Overlain by Frere Formation or Sweetwaters Well Dolomite. Underlain unconformably by Maraloou Formation/Mooloogool Group.|Sandstone, siltstone and minor conglomerate, and locally, stromatolitic carbonate and chert breccia.|30-AUG-19
20942|Yelma Formation|71798|6|Mentioned|p110|||Earaheedy Basin.||Tooloo Group||||
20942|Yelma Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 2027+/-23 Ma, min 1811+/-13 Ma|Tooloo Group|||Sandstone, dolomite (locally stromatolitic), siltstone, and shale; minor conglomerate and limestone.|
20949|Yenart Sands|29631|6|Mentioned|p58|||||||||
20984|Yilgangi Conglomerate|22450|6|Mentioned|p21||Archean|Yilgarn Craton.||||||07-NOV-08
20984|Yilgangi Conglomerate|23457|6|Mentioned|p81|||||||||
20984|Yilgangi Conglomerate|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
20984|Yilgangi Conglomerate|24196|6|Mentioned|p47 Fig.5|||Geological Province: Murrin Domain, Yilgarn Craton.||||||
20984|Yilgangi Conglomerate|24494|6|Mentioned|p14|||||||||
20984|Yilgangi Conglomerate|36869|6|Mentioned|p48|||||||||
20984|Yilgangi Conglomerate|60555|5|Briefly described|p2 Fig. 1, p6 Fig. 3|Archean|Archean|Age: <2662+/-4Ma. Thickness: 935m. Intruded by a graniodiorite (2662+/-4Ma). Polymictic clast-supported (cobble-pebble) conglomerates, massive to weakly graded sandstones. Submarine fan.||||||30-NOV-09
20984|Yilgangi Conglomerate|64340|6|Mentioned|p2 Fig. 1|||||||||
20984|Yilgangi Conglomerate|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)||||Weakly metamorphosed polymictic conglomerate, poorly sorted, moderately well-rounded.|
20984|Yilgangi Conglomerate|65264|5|Briefly described|p21|||Geological province: Kurnalpi terrane.||||||07-FEB-11
20984|Yilgangi Conglomerate|72049|5|Briefly described|p256, p270|||Geochronology analyses, results, and interpretation are discussed in detail.||Late Merougil Group||||
20999|Yindagindy Formation|6944|6|Mentioned|p584.|||Southern Carnarvon Basin. Dolomite. Overlies Gneudna Formation.||||||27-OCT-14
20999|Yindagindy Formation|12733|6|Mentioned|p554 Fig.2.|Early Carboniferous|Early Carboniferous|Visean.||||Overlies Williambury Sandstone. Is overlain by Quail Formation.||
20999|Yindagindy Formation|14228|5|Briefly described|p5 fig2, p6 fig3, p7, p18|Visean|Visean|Merlinleigh Sub-basin.||||Overlies Williambury Formation.|Sandstone and limestone.|
20999|Yindagindy Formation|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
20999|Yindagindy Formation|23311|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|||||||
20999|Yindagindy Formation|23312|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|||||||
20999|Yindagindy Formation|23403|4|Described|p7|Early Carboniferous|Middle Devonian|Geological Province: Gascoyne Complex.||||||24-NOV-09
20999|Yindagindy Formation|23726|6|Mentioned|p31|Early Carboniferous|Early Carboniferous|Underlying unit Williambury Formation Geological Province: Carnarvon Basin.||||||
20999|Yindagindy Formation|23815|4|Described|p277, 278|Visean|Visean|Geological Province: Carnarvon Basin. Overlying units: Harris Sandstone (disconformable) and Lyons Group. Underlying unit: Williambury Formation (conformable). Max. thickness: 115 m. Richly fossiliferous.||||||27-APR-05
20999|Yindagindy Formation|24059|5|Briefly described|p146|Early Carboniferous|Early Carboniferous|Geological Province: Carnarvon Basin.||||||
20999|Yindagindy Formation|24390|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
20999|Yindagindy Formation|30875|6|Mentioned|p10|||Carboniferous age||||||
20999|Yindagindy Formation|31561|5|Briefly described|p34|||See also P33. Early Carboniferous||||||
20999|Yindagindy Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
20999|Yindagindy Formation|32648|6|Mentioned|p32|||Visean||||||
20999|Yindagindy Formation|32789|3|Fully described|p82|||Refers Condon (1954). L.Carb.||||||
20999|Yindagindy Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
20999|Yindagindy Formation|33386|6|Mentioned|Fig.7|||||||||
20999|Yindagindy Formation|33453|5|Briefly described|p70|||Carb.||||||
20999|Yindagindy Formation|35282|6|Mentioned|Fig.2|||||||||
20999|Yindagindy Formation|35981|6|Mentioned|p134|||||||||
20999|Yindagindy Formation|36115|6|Mentioned|p137|||||||||
20999|Yindagindy Formation|36257|6|Mentioned|Table 2.1|||||||||
20999|Yindagindy Formation|36890|3|Fully described|p277|||Formerly Yindagindi Limestone.||||||15-DEC-08
20999|Yindagindy Formation|40617|6|Mentioned|p4|||Also Mention Fig.1||||||
20999|Yindagindy Formation|40992|6|Mentioned|Fig.8|||||||||
20999|Yindagindy Formation|41271|6|Mentioned|p209|||||||||
20999|Yindagindy Formation|41438|6|Mentioned|p103|||||||||
20999|Yindagindy Formation|41443|6|Mentioned|p163|||||||||
20999|Yindagindy Formation|41839|4|Described|p20|||Formerly "Yindagindi Limestone"||||||
20999|Yindagindy Formation|42116|4|Described|p30|||||||||
20999|Yindagindy Formation|42547|6|Mentioned|p89|||Misspelling of Yindagindi Formation? or is this correct spelling?||||||
20999|Yindagindy Formation|42994|6|Mentioned|p127|||||||||
20999|Yindagindy Formation|43566|6|Mentioned|p413|||||||||
20999|Yindagindy Formation|44344|14|Not recorded|p.6,7,19,opp.4,map|||Carboniferous in age.||||||
20999|Yindagindy Formation|44345|14|Not recorded|map legend||Early Carboniferous|Lower Carboniferous.||||||
20999|Yindagindy Formation|44537|14|Not recorded|map legend|||? Upper Carboniferous.||||||
20999|Yindagindy Formation|44657|14|Not recorded|p.5,7,8|||||||||
20999|Yindagindy Formation|44993|14|Not recorded|p.7,14|||Camaratoechia.||||||
20999|Yindagindy Formation|44994|5|Briefly described|p9|||Fig.6 Correlation.||||||
20999|Yindagindy Formation|45015|2|Defined|p72-77, map legend|Early Carboniferous|Early Carboniferous|Dominant pebbly quartzwacke and intercalated thin hard limestone beds. Conformably overlies Williambury Fm; disconformably underlies Harris Sandstone or unconformably beneath Lyons Group. Max. thickness: 300ft. Geological Province: Carnarvon Basin.||||||29-JAN-08
20999|Yindagindy Formation|45016|14|Not recorded|p.16,18||Early Carboniferous|L.Carboniferous. p.7,9,10,11,21,25,29,Fig.48.||||||
20999|Yindagindy Formation|45063|6|Mentioned|p22|||Carb.||||||
20999|Yindagindy Formation|45097|6|Mentioned|Fig.|||Few brachiopods ?Visean. Correlation chart||||||
20999|Yindagindy Formation|45169|6|Mentioned|p1|||||||||
20999|Yindagindy Formation|48831|14|Not recorded|Not recorded|||||||||
20999|Yindagindy Formation|48971|6|Mentioned|p33|||See also P42.||||||
20999|Yindagindy Formation|49942|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Geological Province: Merlinleigh Sub-basin.||||||
20999|Yindagindy Formation|50085|5|Briefly described|p19 Fig. 10|Carboniferous|Carboniferous|Geological Province: Southern Carnarvon Basin.||||||
20999|Yindagindy Formation|60384|5|Briefly described|p244|Early Permian|Carboniferous|Merlinleigh Sub-Basin, Southern Carnarvon Basin. Marine siliciclastics.||||||15-NOV-12
20999|Yindagindy Formation|60725|5|Briefly described|p29 Fig.2, p30, p35 Fig.5, p36 Fig.6. |Carboniferous|Carboniferous|||||||
20999|Yindagindy Formation|64580|6|Mentioned|map legend|||Carboniferous succession, Southern Carnarvon Basin.||||||15-DEC-08
20999|Yindagindy Formation|64972|6|Mentioned|p617 Fig. 5|Carboniferous|Carboniferous|||||||
20999|Yindagindy Formation|65382|6|Mentioned|p717 App. 2|Visean|Visean|Carnarvon Basin. 327 Ma||||||
20999|Yindagindy Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark blue/grey calcareous mudstone.|
20999|Yindagindy Formation|67200|5|Briefly described|p7 fig 5,p18 table 1, p48, p55, app 2 p7|Carboniferous|Carboniferous|Thermal conductivity of 3.80 W/mK||||Overlies Williambury Formation|Parallel and planar cross bedded sandstone, siltstone and limestone; calcareous mudstone.|
20999|Yindagindy Formation|69011|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlain by the Lyons Group. Underlain by the Williambury Formation.|Comprises quartzose, lithic, and calcareous sandstone; lesser calcilutite and calcarenite.|28-APR-14
20999|Yindagindy Formation|69029|6|Mentioned|p326|Visean|Visean|Of onshore Carnarvon Basin.||||Overlain by Quail Formation. Underlain by Williambury Sandstone.||
20999|Yindagindy Formation|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Early Carboniferous|Early Carboniferous|Carnarvon Basin. Deposited in shallow marine conditions. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.||||Overlies the Williambury Formation. Overlain by the Quail Formation.|Sandstone and limestone.|
20999|Yindagindy Formation|70138|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||Overlies Williambury Formation. Is overlain by Harris Sandstone (Lyons Group).|Quartzose, lithic, and calcareous sandstone; lesser calcilutite and calcarenite.|
20999|Yindagindy Formation|70795|4|Described|100k_geologyp_lut.csv|Visean|Visean|Also 100k_interpgeop_lut.csv|347-331 Ma||||Quartzose, lithic, and calcareous sandstone; lesser calcilutite and calcarenite.|
20999|Yindagindy Formation|70826|6|Mentioned|p6 tbl 3|Carboniferous|Carboniferous|Southern Carnarvon Basin.||||||
20999|Yindagindy Formation|71146|5|Briefly described|p6, p34|Visean|Visean|Southern Carnarvon Basin.||||Overlies the Williambury Formation. Unconformably overlain by the Harris Sandstone and the Quail Formation.|Carbonate and mudstone.|
20999|Yindagindy Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, limestone, mudstone|
20999|Yindagindy Formation|73117|6|Mentioned|p15|Visean|Visean|||||Underlain by Williambury Formation.||
21004|Yindi Monzogranite|42741|5|Briefly described|map legend|Archean||||||||07-NOV-08
21004|Yindi Monzogranite|43075|5|Briefly described|p9|||||||||
21004|Yindi Monzogranite|43222|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21004|Yindi Monzogranite|43294|5|Briefly described|p8||Archean|||||||07-NOV-08
21004|Yindi Monzogranite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
21004|Yindi Monzogranite|60076|5|Briefly described|p46 App. 1|||[Agmyi]   Fine- to medium-grained, equigranular monzogranite.||||||
21004|Yindi Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Fine- to medium-grained, equigranular monzogranite.||||||07-FEB-11
21004|Yindi Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine- to medium-grained, equigranular monzogranite.|07-AUG-15
21004|Yindi Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Recrystallized monzogranite and granodiorite. Fine- to medium-grained, equigranular monzogranite.|
21004|Yindi Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
21004|Yindi 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 monzogranite|
21066|Yulleroo Formation|42930|5|Briefly described|Fig.1 p473|Carboniferous|Early Carboniferous|Lateral equivalent to Laurel Formation. In the Fitzroy Trough. Geological province: Canning Basin.||||||13-NOV-07
21066|Yulleroo Formation|45153|6|Mentioned|App.3-43|||||||||
21066|Yulleroo Formation|69182|6|Mentioned|Ch4 p63 |||Canning Basin.||Fairfield Group||||
21089|Zimmermann Sandstone|32648|6|Mentioned|p32|||L.Carb.||||||
21089|Zimmermann Sandstone|32699|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Quartz sandstone and siltstone.||||||02-DEC-04
21089|Zimmermann Sandstone|34085|6|Mentioned|Cor.chart|||Tourn. - Visean||||||
21089|Zimmermann Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
21089|Zimmermann Sandstone|36890|3|Fully described|p380|||||||||
21089|Zimmermann Sandstone|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
21089|Zimmermann Sandstone|42547|4|Described|p101|||||||||
21089|Zimmermann Sandstone|44994|6|Mentioned|Fig.6|||Correlation. See also p14.||||||21-DEC-06
21089|Zimmermann Sandstone|45038|2|Defined|p.86||Early Carboniferous|See also Figures and Plates. L.Carb.||||||21-DEC-06
21089|Zimmermann Sandstone|45039|6|Mentioned|p27|||Lower Carboniferous. See also p33.||||||21-DEC-06
21089|Zimmermann Sandstone|45063|6|Mentioned|p8|||See also p19 and Fig. 3. L.Carb.||||||21-DEC-06
21089|Zimmermann Sandstone|60364|4|Described|p184|Visean|Tournaisian|Of Langfield Group. Disconformably overlies Septimus Limestone. Disconformably overlain by Border Creek Formation. Quartz sandstone. Thickness in type section: 140m. Contains fossils. Ostracods described. Geological Province: Bonaparte Basin.||||||11-MAY-05
21089|Zimmermann Sandstone|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
21089|Zimmermann Sandstone|64694|5|Briefly described|p233, p234 Fig.2, p254 Fig.12|Tournaisian|Tournaisian|Burt Range Shelf, Onshore Bonaparte Basin.||Unit in Langfield Group.||Disconformably overlies the Septimus Limestone.||
21089|Zimmermann Sandstone|69452|3|Fully described|p36:12 Fig.36.12|Tournaisian|Tournaisian|Veevers and Roberts (1968). Petrel Sub-basin, Bonaparte Basin. The type section is at Mount Zimmermann, central Burt Range in WA, where it is 133m thick. Rapidly thins away from this area. Less than 30m thick in NT. Also crops out in Keep River National Park (NT). Shoreface and shallow-marine deposits. Uncommon marine fossils include brachiopods, bivalves, bryozoans, crinoids and trace fossils (Rhizocorallium). Onshore. See also references to [mis-spelt] Zimmerman Sandstone (36:6 Fig.36.5; 36:9, 12-14).||Langfield Group.||Conformably overlies Septimus Limestone. Is overlain by Keep Inlet and Border Creek Formations unconformably or disconformably.|Brown to white quartz sandstone with interbedded white siltstone in the upper part. NT exposures are friable, medium-grained, slightly calcareous sandstone; some beds almost entirely quartzose; others contain quartz, feldspar and lithic grains.|12-JUL-16
21089|Zimmermann Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Quartzose, feldspathic and lithic sandstone, minor siltstone and shale|
