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
29945|50-mile Tank Gneiss|43052|5|Briefly described|Fig.3.8|||Misspelling of Fifty Mile Tank Gneiss.||||||
81429|AK1 Lamproite|70731|6|Mentioned|p268|Stenian|Stenian|Geological province: King Leopold Orogen and Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
42469|AWB komatiites|60696|6|Mentioned|p346|||Informal reference to the komatiites of the Agnew-Wiluna (Greenstone) Belt.||||||
42151|Abadare Dolerite|50622|6|Mentioned|p316 Fig.3|||||||||
68159|Aberadre Dolerite|60626|6|Mentioned|p55|||Equivalent to Golden Mile Dolerite.||||||
69592|Abrakarrie Limestone|61155|5|Briefly described|p17|Early Miocene|Late Oligocene|Misspelt - see Abrakurrie Limestone (place-name is Abrakurrie Cave in WA). Age: 25-20.5Ma. Max. thickness: 90m. Geological Province: Eucla Basin.||||||
25755|Abydos Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
25755|Abydos Adamellite|39697|3|Fully described|p39|||||||||
25755|Abydos Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||160 sq. km. Post-tectonic granitoid.||Yule Granitoid Complex||Intruded by Woodstock Adamellite.|Porphyritic biotite monzogranite, foliated.|
40303|Acacia Sandstone|24390|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
40303|Acacia Sandstone|50085|5|Briefly described|p6 Fig. 4|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
40303|Acacia Sandstone|61023|5|Briefly described|p10 Fig. 6|Ordovician|Ordovician|Geological Province: Canning Basin.||||||11-APR-08
40303|Acacia Sandstone|61551|6|Mentioned|p359.|||Is a hydrocarbon reservoir in the sub-salt play in the Blina oil field.||||||
40303|Acacia Sandstone|64982|4|Described|p695, p701, p704 Fig.9.|Ordovician|Ordovician|South Canning Basin. Formal name includes its rank of Member. The 1996 Looma 1 exploration well encountered low-permeability oil-bearing intervals. Sealed by Willara Formation carbonates. Article details the petrography.||Unit in Willara Formation.|||Monocrystalline quartz sandstone, grains subangular fine to well-rounded medium.|
40303|Acacia Sandstone|67888|6|Mentioned|p82|||||||||
40303|Acacia Sandstone|73344|6|Mentioned|Pl.2|||[Probably an abbreviation of Acacia Sandstone Member].||||||
39286|Acacia Sandstones|24246|5|Briefly described|p16|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
39286|Acacia Sandstones|24376|5|Briefly described|p11|Ordovician|Ordovician|Geological Province: Canning Basin||||||02-MAR-05
69148|Acacia sandstone|61139|5|Briefly described|p42|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
81158|Acacia sandstone member|69883|5|Briefly described|p5-p6, p14, 18, 21, 42, Plate 4|||Originally of Little, 1992, King,  1998.Canning Basin. Informal. Also referred to as the 'Acacia sands' on p5. Forms a significant central body of the Willara Formation in the central and eastern areas of the basin. Has reservoir potential and has been associated with significant hydrocarbon shows. See also plate 4.||Of Willara Formation.||||26-FEB-20
38556|Actinolite-Sulfide Schist Marker Unit|24395|4|Described|p207, p211|||Informal name of Barnes et al, 1986.||||||
40501|Ada Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton.||||||07-NOV-08
83071|Agnew Greenstone Sequence|73151|6|Mentioned|p2|||Of Duuring et al., 2010, (equivalent to basal Kalgoorlie Group). See also Agnew sequence on p14.||||Equivalent to Kalgoorlie Group||
77543|Agnew Sequence|66880|6|Mentioned|p8, p26.|Archean|Archean|Mafics/ultramafics. Correlative with Kambalda Sequence.||||||
42471|Agnew komatiite|60696|6|Mentioned|p351|||Informal reference to the komatiite in the Agnew-Wiluna Greenstone Belt.||||||
42471|Agnew komatiite|69583|5|Briefly described|p39|||Informal name for a prominent marker unit in the Agnew-Mount White district. Considered to be contemporaneous with the Kambalda Komatiite.|||||A thick unit of komatiite with minor komatiitic basalt layers.|
80971|Aileron Province granitic unit 80971|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen. Age inferred. |||||Granitic rock.|
73598|Airport Ultramafic Unit|63459|5|Briefly described|p802, p803 Fig.1|Archean|Archean|Of Hunter et al (1994). Local name for ultramafic unit in eastern ca.2.7Ga  Agnew-Wiluna Greenstone Belt; Hayes Well Ultramafic Unit is in west. Geol.Prov: Yilgarn Craton. Incl: layered melagabbros and gabbronorites. See also p807, p818 Fig. 8, p821 Tb. 7||||||07-NOV-08
83714|Airport ultramafic unit|70275|5|Briefly described|p478, 480|||Leinster area, Agnew-Wiluna Belt, Yilgarn Craton. Thrusting produced duplication of this unit.|||||Consists largely of thin flow komatiite sequences; local thicker cumulate unit. Has a three-pronged shape as a result of repeated thrusting.|
75614|Ajana Sandstone|65313|6|Mentioned|p579|||Coburn 1 well. See Ajana Formation (p578, p579).||||||26-MAR-12
29230|Ajax Seam|36265|5|Briefly described|Fig.3.28|Early Permian|Early Permian|Part of the Ewington Member (Collie Coal Measures). Geological province: Collie Basin.||||||04-MAR-08
29230|Ajax Seam|38936|6|Mentioned|p323|||||||||
38789|Ajax suite|23926|6|Mentioned|p9|||Informal.  Geological Province: Yilgarn Craton.||||||
41028|Alabama sandstone|24196|5|Briefly described|p51|Archean|Archean|Informal - see Alabama Sandstone. Age: 2662 +/- 4 Ma. Geological Province: Laverton domain, Yilgarn Craton.||||||07-NOV-08
68048|Albany Enderbite|24526|5|Briefly described|p105 Fig. 6, p108|Mesoproterozoic|Mesoproterozoic|Of the Nornalup Complex.  Age: 1289+/-10Ma.  May not be intended as a formal name?||||||01-MAR-05
68048|Albany Enderbite|62381|5|Briefly described|p3 Fig.3.|||See Albany Adamellite.||Unit in Nornalup Complex.||||
80173|Alcurra Dolerite Suite|71211|6|Mentioned|p64, p85, p104, p105|Stenian|Stenian|On the basis of geochemistry is interpreted to be genetically related to the Rowland Suite and the Hogarth Formation. Interpreted to have formed from the melting of upwelling mantle material that then ascended to the base of the lower crust and thereafter the middle to upper crust thus forming the magma chamber from which the Rowland Suite and Pussy Cat Group units formed. See also  p108 fig 3.11, p110-p113, p118. Shown as Alcurra Dolerite (Suite) p9, 26.|1067 +/- 8 Ma (Kirkland et al., 2009)|||||03-OCT-17
80437|Alcurra Dolerite suite|69655|5|Briefly described|p2, p6, p24, p34, p39|Stenian|Stenian|See also p42, p44-p46, p48, p57-p58, p62, p77-p78. Musgrave Province. Informal name. Geochemistry and mineralisation potential discussed in some detail. See also Alcurra suite p30, Alcurra Dolerites p34, Alcurra Dolerite p43, Alcurra dolerite p78.|1067 Ma|Warakurna Supersuite||Intrudes the Kunmarnara and Tollu Groups.|Fine- to medium-grained olivine gabbro, olivine norite, ferronorite and ferrodiorite.|03-APR-18
77416|Alcurra Dolerites|65693|5|Briefly described|p7.|||Use of the plural is unexplained.||Unit in Alcurra Suite.||||
77416|Alcurra Dolerites|72476|5|Briefly described|p25|||Musgrave Province. See also references to Alcurra Dolerite (p35, 39).|~1080-1040 Ma.||||Dolerite dykes.|
77417|Alcurra Suite|65693|4|Described|p1, pp8-15.|||See also Alcurra suite. Ophitic. Appears to be confined to Musgrave Province. Compositionally distinct from other mafic units of Warakurna Supersuite. Linked to some (if not all) orthomagmatic Ni-Cu-PGE mineralization in Musgrave Province.|||Includes Alcurra Dolerite.||Relatively evolved, Fe-rich, incompatible trace element-rich suite of tholeiitic intrusions.|22-APR-20
77417|Alcurra Suite|65907|5|Briefly described|p6, p34.|||Mafic magmatism; hosts world class orthomagmatic Ni-Cu mineralisation. Called Alcurra dyke suite in places in the Report.|1068-1067 Ma.|||||
77417|Alcurra Suite|67128|4|Described|p5 Fig.3, p11, p28-29|||Western Musgrave Province. Related to the Giles Event. Locally associated with Cu mineralisation.|1068 +/- 4 Ma, 1067 +/- 8 Ma.|Warakurna Supersuite.|Saturn gabbro.||An evolved, Fe-rich, and incompatible trace element rich suite of tholeiite dolerite, ferrodiorite, ferronorite, gabbro and olivine-gabbro dykes and sills. A variety of textures and settings.|
42406|Alcurra dyke swarm|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mafic. Geological Province: Musgrave Block.||||||22-FEB-05
77418|Alcurra suite|65693|4|Described|p1, pp8-15.|||Used throughout the article as alternative to Alcurra Suite. Geochemistry and Nd isotopic signatures in west Mulgrave Province are similar to those of Alcurra dykes of the Northern Territory.|||Includes Alcurra Dolerite.||Relatively evolved, Fe-rich, incompatible trace element-rich suite of tholeiitic intrusions.|22-APR-20
77418|Alcurra suite|69655|6|Mentioned|p30||||||||Gabbroic rocks.|
32724|Alexander beds|44997|14|Not recorded|p.37|||||||||
41029|Alicia syenogranite|24196|5|Briefly described|p44|Archean|Archean|Informal name. Age: 2693 +/- 3 Ma (Fletcher et al., 2001). Geological Province: Yilgarn Craton.||||||07-NOV-08
41365|Allanah Suite|50607|6|Mentioned|p2.3, 2.5|||Geological Province: Musgrave Block.||||||
75507|Allandale Sandstone|64630|5|Briefly described|p31 Fig.2|Kungurian|Kungurian|N.B. Not the Allandale Formation of NSW. Province: Collie Subbasin. Overlies the Ewington Coal Measures, underlies the Premier Coal Measures. Palynology age: P.sinuosis. Correlates with the middle of the Redgate Coal Measures.||||||18-JAN-10
75507|Allandale Sandstone|70774|5|Briefly described|p5 fig 3|Kungurian|Kungurian|Collie Basin.||||Overlies the Ewington Coal Measures. Overlain by the Premier Coal Measures.||
42407|Amata dyke swarm|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mafic. Geological Province: Musgrave Block.||||||22-FEB-05
42407|Amata dyke swarm|63562|6|Mentioned|p337, p341|||Of Musgrave Inlier. Plume-related magmatism. Other ages are 790 +/- 40 Ma and 797 +/- 49 Ma (Sm-Nd: Zhao et al., 1994).|824+/-4 Ma baddeleyite U-Pb (Glikson et al. 1996)|||||
42407|Amata dyke swarm|69437|5|Briefly described|p22:3|||Of the Gairdner Large Igneous Province.  Intrudes Supersequence 1 in the Officer and Amadeus Basins.|c.825 Ma.|||||12-JUL-16
42407|Amata dyke swarm|69873|6|Mentioned|p73|||Possible equivalent of Tayatea Dyke Swarm in Tasmania.||||||
42407|Amata dyke swarm|72259|6|Mentioned|p1, p9|||[Written as Gairdner-Amata dyke swarm and Gairdner-Amata Dyke (G-A) dyke swarm].||||||
78327|Amata dykes|65135|5|Briefly described|p17|Cryogenian|Cryogenian|Informal name. Linked with the Gairdner dykes on the basis of similar ages and chemistry (Glikson et al., 1996). Sm-Nd age of 790 +/- 40 Ma (Zhao et al., 1994)||||||
78327|Amata dykes|67128|5|Briefly described|p8|||Musgrave Province.|c.800 Ma.||||Mafic dykes.|
78327|Amata dykes|70083|6|Mentioned|p207|||Intrudes much of the Musgrave Inlier.|c.800 Ma.||||Dolerite.|
30672|Amherst Metamorphics|22754|4|Described|p6|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.||||||07-NOV-08
30672|Amherst Metamorphics|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
30672|Amherst Metamorphics|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen. Thought to represent metamorphosed equivalents to the Marboo Formation. Metamorphosed to LPHT conditions between 1860 and 1805 Ma.|||||Migmatised paragneisses and orthogneiss.|
30672|Amherst Metamorphics|64580|4|Described|map legend||Paleoproterozoic|Biotite-hornblende granodiorite gneiss; metamorphosed NEVILLE GRANODIORITE? Qtz-musc-biot-andalusite-sillimanite-garnet-cordierite-K-feldspar-plag schist, granofels, and migmatite; metamorphosed MARBOO FORMATION.||||||15-DEC-08
30672|Amherst Metamorphics|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Biotite-hornblende granodiorite gneiss. Schist, granofels and migmatite.|
39285|Anderson Sandstone|24246|6|Mentioned|p14|||Geological Province: Canning Basin.||||||
77523|Andover Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
83224|Andrews Formation|73445|5|Briefly described|p10, 12|||Canning Basin. These rocks, possibly of this Formation, were intersected at 2000-2500m in the Point Moody No.1 well. Age is given as ?lower Carboniferous.||||Is overlain by the Grant Group.|Sandstone, siltstone and shale.|
80990|Angas Hill Formation|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1). [misspelling of Angas Hills Formation.]|||||Interbedded conglomerate and sandstone, minor mudstone.|
75569|Angas Hills beds|65074|4|Described|p351 fig 4-37, p353, p358-360, p362|Devonian|Devonian|Of SW Birrindudu Basin. 300 m thick. Type section details given. Non-fossiliferous. Forms series of cuestas and mesas.||||Probably equivalent to Pedestal beds and Chuall beds.|Interbedded conglomerate and sandstone with minor mudstone.|
75569|Angas Hills beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, mudstone|
38772|Angeles Shale|23890|5|Briefly described|p9|Paleoproterozoic|Archean|Of Wittenoom Formation, Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
77409|Angelo Granite|65417|6|Mentioned|p156.|||||||||
79829|Angus Hills beds|69031|5|Briefly described|p9|||Amadeus Basin outlier overlying the west Arunta Orogen. Previously correlated with Pertnjara Group; recent work suggests it is part of the older Petermann Orogeny succession.|||||A succession of immature, red-brown sandstone and conglomerate.|
32731|Anketell-Parda Formation|44998|14|Not recorded|p.121,127,164|Albian|Neocomian|(Samphire Marsh & BMR Wallal 4 bores). Neocomian-Aptian-Albian. See also p164-6, 188-9.||||||
70178|Antarctic Chert Member|61560|5|Briefly described|p498 Tb. 4|||Of the Apex Basalt. Displays impact spherules caused by impact ejecta. Geological Province: north Pilbara Block.||||||10-MAY-06
70178|Antarctic Chert Member|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Of the upper Warrawoona Group.  Age: 3.47Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
70178|Antarctic Chert Member|65757|5|Briefly described|p82 Fig.1|||Same sample shown as Antarctic Creek Member p81. Diamictite, chert, arenite, felsic volcanics, dolerite, jaspilite, base Apex Basalt.||||||06-OCT-15
70212|Antarctic Creek cherts|61579|6|Mentioned|p61|||Informal name. Of the North Pole area (WA). ||||||
32458|Antrim Plateaux volcanics|44159|5|Briefly described|Table p.38||Early Cambrian|||||||
70213|Apex Basalt, Lower|61579|6|Mentioned|p59 Fig. 3|||Informal - see Apex Basalt.||||||
70214|Apex Basalt, Upper|61579|6|Mentioned|p59 Fig. 3|||Informal - see Apex Basalt.||||||
69902|Apex Chert|61256|6|Mentioned|p342|||||||||
69902|Apex Chert|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Informal name - refers to cherty part of Apex Basalt. See Apex Basalt.||||||07-FEB-11
69902|Apex Chert|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.46 Ga.|Warrawoona Group.||||
69902|Apex Chert|71137|6|Mentioned|p14|Archean|Archean||3.5 Ga.|||||
40502|Apex Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group).  Geological Province: Pilbara Craton.||||||07-NOV-08
40502|Apex Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Altered basalts, chert. Max. thickness: 4km. Geological Province: Pilbara Craton.||||||07-FEB-11
40502|Apex Formation|60636|5|Briefly described|p44, p52|Archean|Archean|Of the Warrawoona Group. Predominantly plagioclase porphyry. Underlies Panorama Formation; overlies Duffer Formation. Age: 3459+/-2Ma. Name used interchangeably with Apex Basalt. See also p35-36 Fig. 3.2.||||||07-FEB-11
40502|Apex Formation|62427|5|Briefly described|p3 Fig.2, p4, p6 Fig.3, p12 |Paleoarchean|Paleoarchean|Also called Apex Basalt, evidently interchangeably.|3459 +/- 2 Ma.|Of the Warrawoona Group|||Basalt|
35693|Apex chert|63245|6|Mentioned|p11|||Informal name for chert associated with Apex Basalt of the Warrawoona Group.||||||
35693|Apex chert|66109|6|Mentioned|p192, 202|Paleoarchean|Paleoarchean|Biological origin of putative fossil filamentous microfossils - the oldest diverse assemblage of microfossils known - has been confirmed. Optical photomicrographs, Raman kerogen images, and confocal laser scanning micrographs of bona fide microfossils.|3465 Ma.|||||
35693|Apex chert|67668|5|Briefly described|p.154, 162,||Paleoarchean|Informal. Occurs within/in association with the Apex Basalt. Presented as 'Apex chert' on p154.|c.3460 Ma|Warrawoona Group||||
35693|Apex chert|68207|6|Mentioned|p761-769|||NW Pilbara Craton. This study confirms the biogenicity of the microbe fossils and associated components in this unit. CLSM, 2D and 3D Raman images, C isotope graphs.|c.3465 Ma.||||A brecciated and altered hydrothermal vein deposit.|
35693|Apex chert|69569|5|Briefly described|p284-285, 287-288|||Brassier et al. (2011). Marble Bar greenstone belt, East Pilbara Terrane. Described as an informal name. The authors conclude that carbonaceous material is not unambiguously  evidence of life, but may result from post-depositional hydrothermal remobilisation and redeposition.||Apex Basalt.|||A stratiform chert layer.|
35693|Apex chert|70507|6|Mentioned|p444-445|Archean|Archean|Geological province: Pilbara Craton.||||||
35693|Apex chert|70729|3|Fully described|p161-163,165,171,174-176|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Informally referring to the lowermost, thickest of the stratiform chert horizons of the Apex Basalt. Thickness: 10-15m. Equivalent to unit 4 of Brasier et al., 2005, 2011. Likely to have been deposited in a protected shallow marine environment adjacent active volcanoes, as suggested by ashfall volcanic components. Carbonaceous microstructures include: (i) primary laminated grains; (ii) filament-like laminae entraining sediment grains; (iii) roll-up structures; and (iv) flaky grains. Collectively, they resemble a suite of microscopic microbially induced sedimentary structures (MISSs) of Noffke (2009, 2010). Possible evidence of geologically plausible environment for microbial life, suggests that such features have a biological origin.||Unit of Apex Basalt.|||(i) carbonaceous laminated microgranular chert; (ii) laminated black, grey and white chert; (iii) metalliferous (Fe-rich) chert; (iv) clotted carbonaceous chert; and (v) silicified volcaniclastics.|
35693|Apex chert|70834|5|Briefly described|p296-305, 312|||Informal name. Marble Bar area, Pilbara Craton. Putative filamentous microstructures (""microfossils"") are not from this horizon, but from hydrothermally influenced black chert veins 100m lower.|3.46 Ga.|||Intrudes lower part of Apex Basalt.|Thin stratiform chert horizon.|
79797|Apex chert""|67270|4|Described|p1-60|Paleoarchean|Paleoarchean|Informal and invalid name (Schopf and Packer, 1987). Chinaman Creek, c.5 km W of Marble Bar. Contains carbonaceous structures accepted as the Earth's oldest known microfossils; this article reinforces the argument that they are in fact of geological origin. Cross-cut by hydrothermal silica "chert" veins. Lithology described in detail.|c.3460 Ma.|Apex Basalt.|||A stratiform unit of bedded grey to black chert, with associated mafic-felsic volcaniclastic rocks.|
70215|Apex cherts|61579|6|Mentioned|p81|||Informal name. See also Apex chert. ||||||
79238|Aranoo Sandstone Member|70097|5|Briefly described|p20 Fig.4|Olenekian||Northern Perth Basin. Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||Kockatea Shale||Overlies Hovea Member.|Sandstone.|30-SEP-16
67851|Arcoona Granite|60076|6|Mentioned|p29 Fig. 7|||In the Edjudina-Laverton greenstones area.||||||
31845|Argyle Basalt|45003|6|Mentioned|p187|||Of Edwards and Clarke (1940). See also Lexicon.||||||04-AUG-08
32787|Argyle lamproite pipe|22547|3|Fully described|p26|Stenian|Stenian|Age: 1177 +/- 47 Ma.||||||14-NOV-06
32787|Argyle lamproite pipe|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Informal name.  Volcaniclastic olivine lamproite intruded by olivine-phlogopite lamproite dykes.  Age: c.1200Ma.||||||
32787|Argyle lamproite pipe|44230|5|Briefly described|Map Legend||Proterozoic|||||||
32787|Argyle lamproite pipe|64580|4|Described|map legend|Mesoproterozoic|Mesoproterozoic|Volcaniclastic olivine lamproite intruded by olivine-phlogopite lamproite dykes.||||||15-DEC-08
39227|Argyle lamproites|23897|6|Mentioned|p378|||Probably Archaean.  Geological Province: Kimberley Block.||||||04-AUG-08
76759|Aries Kimberlite|64722|6|Mentioned|p9||Neoproterozoic|Central Kimberley Basin.|~820 Ma.|||||11-APR-12
76759|Aries Kimberlite|69003|5|Briefly described|p5, p59|Neoproterozoic|Neoproterozoic|Kimberley region, Halls Creek Orogen. One of a number of locally diamondiferous lamprophyres and kimberlites intruded around this time.|c.815 Ma.|||||
76759|Aries Kimberlite|70731|6|Mentioned|p268|Tonian|Tonian|Geological province: King Leopold Orogen and Lamboo Province, Halls Creek Orogen, Kimberley Craton. Associated with Yampi Orogeny.||||||
72570|Aries micaceous kimberlite|62715|5|Briefly described|p1752, p1779|Neoproterozoic|Neoproterozoic|Age: 820+/-20Ma. (Rb-Sr).   Geological Province: Kimberley Basin. See also Aries kimberlite.||||||04-OCT-06
33829|Armanda gabbro|22474|5|Briefly described|p21|Orosirian|Orosirian|Variation of Armanda Intrusion. 1830 Ma||||||
33829|Armanda gabbro|43931|5|Briefly described|p21||Orosirian|1830 Ma. Part of the Armanda Intrusion||||||
31318|Arrino Tuff|45018|14|Not recorded|p40|||||||||
81291|Arrow Stag Formation|69553|5|Briefly described|p62|Mesoproterozoic|Mesoproterozoic|Contains Horodyskia fossils, and possible correlative to the Cassiterite Creek Quartzite of the Balfour Subgroup, but much younger than the Cassiterite Creek Quartzite.|1200-1070 Ma|Unit of Bangemall Supergroup.||||
24671|Arunta complex|38063|6|Mentioned|p28|||||||||
24671|Arunta complex|62082|6|Mentioned|p53|||Informal name.||||||07-FEB-11
23343|Ascot Beds|12759|6|Mentioned|47|||Defined by Playford et al. (1976); redefined as a Formation by Cockbain and Hocking (1989).||||||
23343|Ascot Beds|36293|2|Defined|p205|Pliocene|Pliocene|||||||
23343|Ascot Beds|37307|5|Briefly described|p34|||||||||
23343|Ascot Beds|38774|6|Mentioned|p44|||||||||
23343|Ascot Beds|38775|4|Described|p42|||||||||
23343|Ascot Beds|39834|6|Mentioned|p287|||||||||
23343|Ascot Beds|41538|6|Mentioned|p310|||||||||
23343|Ascot Beds|41783|6|Mentioned|p54|||||||||
39198|Ascot Formation, Lower|23768|5|Briefly described|p30 Fig.6|||Informal - see Ascot Formation.   Geological Province:||||||10-MAR-05
39197|Ascot Formation, Upper|23768|5|Briefly described|p30 Fig.6|||Informal - see Ascot Formation.   Geological Province: Perth Basin.||||||10-MAR-05
73999|Ashbrook Coal Measures|14227|5|Briefly described|Enclos. 2|Artinskian|Artinskian|Of the Sue Group. Overlies Rosabrook Coal Measures; underlies Redgate Coal Measures. Geol. Prov: Bunbury Trough, Perth Basin.||||||07-FEB-11
73999|Ashbrook Coal Measures|71958|5|Briefly described|p34|Roadian|Artinskian|Vlaming Sub-basin.||Sue Group||Overlies the Rosabrook Coal Measures. Overlain by the Redgate Coal Measures.||
67858|Ashburton Formation, Lower|24544|4|Described|p46 Fig.34|Paleoproterozoic|Paleoproterozoic|Sandstone dominant. Thickness: 2.5-5 km. Geological Province: Ashburton Province.||||||07-NOV-08
67858|Ashburton Formation, Lower|71112|5|Briefly described|p75|||Geological province: Pilbara Craton. ||||Overlain by June Hill Volcanics. Underlain by Duck Creek Dolomite.||
67857|Ashburton Formation, Upper|24544|4|Described|p46 Fig.34|Paleoproterozoic|Paleoproterozoic|Mudstone dominant. Thickness: 2.5-6 km. Geological Province: Ashburton Province.||||||07-NOV-08
67857|Ashburton Formation, Upper|71112|5|Briefly described|p73-75|||Geological province: Ashburton Province, Pilbara Craton. Of the Cane River Basin. ||||Underlain (locally unconformably) by June Hill Volcanics.||
68608|Ashburton Formation, upper|50216|6|Mentioned|p208|Paleoproterozoic|Paleoproterozoic|Informal - see the Ashburton Formation. Uppermost part of the Wyloo Group. Age: ca. 1805 Ma (Nelson, 2003).||||||07-NOV-08
32553|Ashburton Group|23774|5|Briefly described|p732|||Name misspelt - actually referring to Ashburton Formation of the Wyloo Group in WA.||||||
32553|Ashburton Group|45373|14|Not recorded|p.177|||||||||
32553|Ashburton Group|48860|14|Not recorded|p.4|||(E53-14/Tennant Creek).||||||
32553|Ashburton Group|64724|5|Briefly described|p46|Paleoproterozoic||Upper part of this group deposited at the same time as the Capricorn Orogeny (1830-1780 Ma)||||||
32553|Ashburton Group|71042|6|Mentioned|p66 fig 2, p98|||||||||24-MAY-19
41030|Auckland granite|24196|5|Briefly described|p69|Archean|Archean|Informal name. Age: 2669 +/- 7 Ma (Black et al., 2002) Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton||||||07-NOV-08
41031|Auckland monzogranite|24196|5|Briefly described|p40|Archean|Archean|Informal name. Age: 2669 +/- 7 Ma (Black et al., 2002). Geological Province: Yilgarn Craton||||||07-NOV-08
68129|Auckland monzogranite""|60416|5|Briefly described|p19|Archean|Archean|Informal name.  Age: 2669+/-7Ma (Cassidy et al 2002). Southwest of the Jasper Flat Mine.||||||07-NOV-08
32752|Austin Greywacke|45015|5|Briefly described|p49, p74, p77|||Rests unconformably on Munabia Sandstone in places; also overlies Moogooree Limestone in places. See also Austin Formation.||||||01-JUN-06
41366|Ayres Range Adamellite|50607|5|Briefly described|p2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Of the Kulgera Supersuite. Age: 1152 +/- 11Ma (SHRIMP, U-Pb).||||||05-FEB-15
40306|B. reticulata Sandstone""|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
40306|B. reticulata Sandstone""|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Informal name.  Geological Province: Northern Carnarvon Basin (Dampier Sub-basin).||||||
40318|B. reticulatum sand|50024|5|Briefly described|p13|Early Cretaceous|Early Cretaceous|Informal name. Sand which is confined to a channel within the middle Barrow Formation - hosts recoverable oil. See also B. reticulatum sand member.  Related to B. reticulatum shales.  Geological Province: Carnarvon Basin.||||||
40319|B. reticulatum sand member|50024|5|Briefly described|p13|||Informal name.  See also B. reticulatum sand which occurs within the middle Barrow Formation.  Geological Province: Carnarvon Basin.||||||
40320|B. reticulatum shales|50024|6|Mentioned|p13|||Informal name.  Related to B. reticulatum sand and B. reticulatum sand member?  Forms a seal to the oil-bearing D. lobispinosum sands. Geological Province: Carnarvon Basin.||||||
39047|BB10|26357|6|Mentioned|not recorded|||||||||
39048|BB11|26357|6|Mentioned|not recorded|||||||||
39049|BB12a|14142|5|Briefly described|p32-35, fig23, Plate2|Albian|Aptian|Age range for BB12 given as  base: Intra-O. operculata dinocyst zone, top: KCCM 33, Lower S. striatoconus dinocyst zone (shown as C. striatoconus in Plate 2. Top of BB12a ~at the boundary between Muderongia tetracantha 2bii and the overlying Muderongia tetracantha 2bi.||||||09-APR-19
39049|BB12a|26357|6|Mentioned|not recorded|||||||||
39050|BB12b|14142|5|Briefly described|p32-35, various figs, Plate2|Albian|Albian|Age range for BB12 given as  base: Intra-O. operculata dinocyst zone, top: KCCM 33, Lower S. striatoconus dinocyst zone (shown as C. striatoconus in Plate 2).||||||09-APR-19
39050|BB12b|26357|6|Mentioned|not recorded|||||||||
39051|BB12c|14142|5|Briefly described|p32-35, various figs, Plate2|Turonian|Albian|Age range for BB12 given as  base: Intra-O. operculata dinocyst zone, top: KCCM 33, Lower S. striatoconus dinocyst zone (shown as C. striatoconus in Plate 2).||||||09-APR-19
39051|BB12c|26357|6|Mentioned|not recorded|||||||||
39052|BB13|26357|6|Mentioned|not recorded|||||||||
39053|BB14|26357|6|Mentioned|not recorded|||||||||
39054|BB15a|26357|6|Mentioned|not recorded|||||||||
39055|BB15b|26357|6|Mentioned|not recorded|||||||||
39056|BB15c|26357|6|Mentioned|not recorded|||||||||
39057|BB16|26357|6|Mentioned|not recorded|||||||||
39058|BB17|14142|6|Mentioned|p122, Fig 23, Plate 2|Eocene|Paleocene|Age range ~ CP7, NP8, H. riedelii to CP11, NP13 D. Iodoensis||||Paritially equivalent to lower parts of Grebe Formation, Prion Formation.||
39058|BB17|26357|6|Mentioned|not recorded|||||||||
39059|BB18|26357|6|Mentioned|not recorded|||||||||
39060|BB19|26357|6|Mentioned|not recorded|||||||||
39061|BB20|14142|6|Mentioned|p122, Fig 23, Plate 2|Miocene|Miocene|Age Range ~CN1b, NN2, S.belemos to CN5, NN6, D.exilis ?||||partial equivalent to Oliver Formation.||
39061|BB20|26357|6|Mentioned|not recorded|||[ Reference: GA REF OREFID = *26357, REFID = 14142 AGSO Record 1997/38.  NOT RefID 26357, which is about onshore drilling near Batchelor , NT.]||||||12-FEB-21
39062|BB21|26357|6|Mentioned|not recorded|||||||||
39063|BB22|26357|6|Mentioned|not recorded|||||||||
35969|BIF 35969|44443|5|Briefly described|map legend|Archean|Archean|Banded iron formation and jaspilite.||||||07-NOV-08
27104|Babbagoola Beds|23914|5|Briefly described|p159|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
27104|Babbagoola Beds|24067|5|Briefly described|p250|Adelaidean|Adelaidean|Geological Province: Officer Basin.||||||
27104|Babbagoola Beds|24161|6|Mentioned|p29|||||||||
27104|Babbagoola Beds|31455|6|Mentioned|p8|||||||||
27104|Babbagoola Beds|31635|6|Mentioned|Table 2|||||||||
27104|Babbagoola Beds|31636|5|Briefly described|p7|||See also Table 2||||||
27104|Babbagoola Beds|31642|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27104|Babbagoola Beds|31914|6|Mentioned|p26|||||||||
27104|Babbagoola Beds|33595|6|Mentioned|p11|||||||||
27104|Babbagoola Beds|34917|6|Mentioned|p12|||||||||
27104|Babbagoola Beds|36096|6|Mentioned|Fig.3|||||||||
27104|Babbagoola Beds|36889|5|Briefly described|p219|||||||||
27104|Babbagoola Beds|36890|3|Fully described|p403|||Formerly Babbagoola Formation||||||
27104|Babbagoola Beds|37460|6|Mentioned|p179|||||||||
27104|Babbagoola Beds|45104|6|Mentioned|p26|||||||||
27104|Babbagoola Beds|45149|2|Defined|p30|Early Cambrian|Early Cambrian|See also Table 1 and P17.||||||
27104|Babbagoola Beds|46975|3|Fully described|p86|||||||||
27104|Babbagoola Beds|49792|5|Briefly described|Fig.5|||||||||
27104|Babbagoola Beds|50204|5|Briefly described|p51|Neoproterozoic|Neoproterozoic|Of the Officer Basin. Name no longer in use. Now of the Kanpa Formation. |||||Siliciclastic and calcareous sedimentary rocks.|06-FEB-18
70755|Babbagoola Beds""|24244|6|Mentioned|p3|||Stated to be the former name for Kanpa Formation (Grey, K., 2002, written comm.)||||||
70755|Babbagoola Beds""|62453|6|Mentioned|p32|||Informal, see Kanpa Formation.||||||
70756|Babbagoola Formation''|62453|6|Mentioned|p32|||Informal, see Kanpa Formation, Wahlgu formation, Lungkarta Formaiton..||||||
26359|Babbagoola beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26359|Babbagoola beds|65363|6|Mentioned|p7.|Neoproterozoic|Neoproterozoic|Named by Townson (1985); these rocks were later referred to as 'McFadden Formation equivalent' (Apak and Moors 2000); subsequently defined as Lungkarta Formation (Grey et al. in prep. at the time of this report).||||||
82135|Babrongan Reef Complex|72497|5|Briefly described|p3 Fig.2.|Famennian|Givetian|Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Unconformably overlies Poulton Formation. Conformably underlies Fairfield Group and laterally equivalent to Clanmeyer Formation and Luluigui Formation.||
28241|Babrongan beds|7433|6|Mentioned|p25 Fig.2. |||Canning Basin.||||||
28241|Babrongan beds|38878|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
28241|Babrongan beds|45158|3|Fully described|p26|||||||||
40740|Backdoor Formation, middle|24183|6|Mentioned|p21|||Thin sandstone unit, equated with the Jeeaila Sandstone Member.||||||
32753|Badgeradda Beds|44142|6|Mentioned|p328 Tb.4-5|||Konecki et al. (1958). Subsequently Badgeradda Group. Formations defined by Perry and Dickins (1960); Williams et al. (1983).||||||
32753|Badgeradda Beds|45015|6|Mentioned|p18|||Of Konecki, Dickens et al, 1958; & Perry & Dickens, 1960 def.).  Superseded by Badgeradda Group.||||||01-JUN-06
32753|Badgeradda Beds|48823|6|Mentioned|p9|||Arenaceous sequence named by Konecki et al (1958). Superseded by Badgeradda Group.||||||
80081|Baja Claystone|69029|6|Mentioned|p319|Albian|Aptian|Of Canning Basin.||||Underlain by Samuel Formation.||
80081|Baja Claystone|69312|5|Briefly described|p3|Albian|Aptian|Canning Basin. ||||Overlies the Samuel Formation.|Shale and claystone.|
79185|Baker Monzogranite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.||Paperbark Supersuite.|||Medium- to fine-grained biotite monzogranite; contains some small mafic inclusions.|
32865|Baker Sandstone|48848|14|Not recorded|p.68|||||||||
41033|Balarky monzogranite|24196|6|Mentioned|p44|||||||||
78855|Bald Hill Member|66129|6|Mentioned|p216 Fig.3|||In Killi Killi Formation?[Probably top of Stubbins Formation]||||||15-MAY-14
78855|Bald Hill Member|66468|6|Mentioned|p17 Fig.4|||Unclear affiliation in figure: appears to overlie Stubbins Formation (or is top of Stubbins Formation?); and appears below Killi Killi Formation.||||||
78855|Bald Hill Member|69003|6|Mentioned|p17 Fig.21|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Diagram lacks clarity: the parent unit may be either Stubbins or Killi Killi Formation, or an un-named dolerite? intrusion.||||||
78855|Bald Hill Member|69426|5|Briefly described|p11:5|Orosirian|Orosirian|200m-thick succession. SHRIMP U-Pb zircon igneous crystallisation age; oldest known unit in the Tanami Group. Not mapped in the NT.|1864 +/- 3 Ma (Bagas et al., 2009).|Stubbins Formation.|||Iron-rich siltstone and shale, carbonaceous shale, chert, pillow basalt, dolerite and minor rhyolite.|12-JUL-16
76801|Bald Hill Sequence|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1865 Ma.|||||
76801|Bald Hill Sequence|70291|4|Described|p178-179,181,186|Orosirian|Orosirian|Geological province: Tanami. Affected by Barramundi Orogeny, leading to high-grade metamorphism.|ca. 1865 Ma|Possibly unit of Tanami Group?||Intruded by high level quartz porphyry, dolerite and minor, high level rhyodacite dated at 1864+\-3 Ma|Basalt and dolerite sills interbedded with turbiditic sandstone and siltstone.|
73775|Bald Hill pegmatite|50542|6|Mentioned|p118|||Informal name. Geological Province: Yilgarn Craton.||||||07-FEB-11
76777|Bald Hill succession|64733|6|Mentioned|p171|||Superseded informal name for Stubbins Formation. Compared with Dead Bullock Formation||||||
29956|Balfour Shale""|43055|6|Mentioned|p25|||Superseded by Balfour Formation.||||||
32616|Bali Gneiss|46311|14|Not recorded|p.6||Archean|Opp. p.6. Archaean (younger)||||||07-NOV-08
32615|Bali Granite|46311|14|Not recorded|p.10||Archean|Archaean (younger). p.10;map.||||||07-NOV-08
37932|Bali Suite|24306|6|Mentioned|p949|||||||||
37932|Bali Suite|65834|6|Mentioned|p17-18, 21, 61|||Witt and Davy (1993). Probable parent granitoids for Li-rich pegmatites in the Coolgardie area.|||Calooli Monzogranite.||Monzogranites.|
29986|Balingup Gneiss Complex|24160|5|Briefly described|p107-108, p113 Fig.49.|Archean|Archean|South-West Terrane, Yilgarn Craton. Metamorphosed to amphibolite, locally granulite, facies.|||||Quartzite, quartz-mica schist, gneiss, BIF; quartzofeldspathic gneisses, amphibolites, calc-silicate gneiss, ultramafic rocks.|
29986|Balingup Gneiss Complex|24410|5|Briefly described|p105, p107 Fig. 58|||Granitic rocks partly recrystallised, greenschist facies. Even-grained, seriate, or porphyritic granites, metasediments, quartzo-feldspathic gneisses, amphibolites, calc-silicate gneiss, ultramafic rocks. Geol. Prov: Yilgarn Craton.||||||
29986|Balingup Gneiss Complex|43061|5|Briefly described|p12|||Age 3.07 - 3.11 Ga. Variation on Balingup Complex?||||||
29986|Balingup Gneiss Complex|44149|5|Briefly described|p14-15, p28-30, p32|Archean|Archean|Mainly metasedimentary rocks; amphibolite to granulite facies. Some ages given.|>3000 Ma||||Interlayered quartzite, quartz-mica schist, quartz-feldspar-biotite-garnet gneiss, BIF; minor quartzo-feldspathic gneiss, amphibolite, calc-silicate gneiss and ultramafic rock. About 30% is orthogneiss. Mostly amphibolite-facies.|
29986|Balingup Gneiss Complex|67861|6|Mentioned|p530|||Possible part source for Collie Basin sediments.||||||
28342|Balla Balla Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
28342|Balla Balla Complex|41594|4|Described|p70|||||||||
73844|Balla Balla Granodiorite|24550|5|Briefly described|p97|||Part of the Balla Balla Granitoid. Migmatitic granodiorite, with pink leucocratic veins; cut by numerous anostomosing shear zones.||||||07-FEB-11
31765|Balla Granite|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane. Coarse-grained, porphyritic to equigranular amphibolite-facies monzogranite, with inclusions of Eurada Gneiss.||||||07-NOV-08
31765|Balla Granite|23574|5|Briefly described|Map Legend|Archean|Archean|Overlain by Churla Granite. Underlain by Impey Granite.||||||07-NOV-08
31765|Balla Granite|23576|5|Briefly described|Map Legend|Archean|Archean|Overlain by Churla Granite. Underlain by Impey Granite.||||||07-NOV-08
31765|Balla Granite|23577|5|Briefly described|Map Legend|Archean|Archean|Overlain by Churla Granite. Underlain by Impey Granite.||||||07-NOV-08
31765|Balla Granite|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: c. 2640 Ma.||||||07-NOV-08
31765|Balla Granite|43835|5|Briefly described|Map Legend|Archean|Archean|Age about 2640Ma.||||||07-NOV-08
31765|Balla Granite|73526|6|Mentioned|p2 Fig.1, p3|Neoarchean|Neoarchean|Western Narryer Terrane. See also Balla granite p4 Tb.1, age of 2638+/-6 Ma.|c. 2640 Ma|||||
24685|Balladonia Beds|33573|5|Briefly described|p405|||||||||
83341|Ballarat Grit|68154|6|Mentioned|p117, 122|||Local name for a  sequence of sandstone and conglomerate.|2693 +/- 18 Ma.|||||
83341|Ballarat Grit|73391|6|Mentioned|p239, Appendix p117, 122.|||Local name for a  sequence of sandstone and conglomerate.|2695 +/- 6 Ma.|||Is intercalated with Ballarat conglomerate sequence. Time-correlated with White Flag Formation.|Dacitic volcaniclastic sandstone with remnant glassy fragments.|
80205|Ballarat member|71166|5|Briefly described|p23 fig 3.16|||[An informal, probable company name from the Kanowna gold camp]. Ballarat Conglomerate discussed on previous page.|||||Polymictic conglomerate, lithic arenite and quartz grit.|05-OCT-17
80205|Ballarat member|73391|4|Described|p132-142, 147, 153, 174, 178, 182|||See also p186-187, 194, 239, 244, 282, 285-286, 347. Kanowna district. Uncertain stratigraphic position. Significant variability in thickness and facies along strike. Described in great detail; stratigraphic columns, photographs, photomicrographs; structures described. May be part of the same depositional unit (Talbot formation) including the Kanowna member. This 2695 Ma age is from a grit sub-unit.|2695 +/- 6 Ma (MDA; Sircombe et al., 2007).|Black Flag Formation.|Ballarat sandstone, Ballarat Conglomerate, Ballarat Grit.|Is faulted over Robinson's Komatiite. Is overlain gradationally by Kanowna member and unconformably by Grave Dam member.|A lower conglomerate/grit sequence, a middle conglomerate sequence, and an upper pebbly sandstone sequence. Total thickness ~500m. Ultramafic and mafic volcanic clasts make up much of the unit.|
83947|Ballarat turbidite|70482|5|Briefly described|p319, 323, 329|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.|2656 +/- 10 Ma (MDA; Squire and Cas, 2006).|Kalgoorlie Sequence.||Conformably overlies Ballarat Conglomerate. Is overlain conformably by Kanowna Conglomerate.|Feldspar-rich volcanic sandstone, siltstone and lesser mudstone.|
79344|Ballona Dolerite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of the Widgiemooltha Large Igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420 - 2400 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2420-2400 Ma (inferred)|Unit of Widgiemooltha Supersuite.|||Dolerite and gabbro; includes cumulate and granophyric differentiates|
78635|Ballona Dyke|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Dolerite and gabbro; includes cumulate and granophyric differentiates.|05-AUG-15
78635|Ballona Dyke|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
78635|Ballona Dyke|71270|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Yilgarn Craton, West Australian Craton.||Unit of Widgiemooltha Dyke Suite.|||Dolerite and gabbro; includes cumulate and granophyric differentiates|
68976|Ballythanna Sandstone|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin||||||
68976|Ballythanna Sandstone|67977|6|Mentioned|p491|||shortening of Ballythanna Sandstone Member in text.||||||
68976|Ballythanna Sandstone|69547|5|Briefly described|p182,192-193,197|Artinskian|Artinskian|Southern Carnarvon Basin. Glacially-influenced succession, and correlable with Winnamea Sandstone and High Cliff Sandstone.||Unit of Callytharra Formation.||||
38567|Bamboo Creek Porphyry""|46319|5|Briefly described|p16|||Informal - see Bamboo Creek Porphyry.||||||
41839|Bamboo Creek Volcanic Member|50544|5|Briefly described|p15 Tb. 1|Archean|Archean|Probably misspelt - see Bamboo Creek Member.  Age: 2756+/-8Ma.||||||07-NOV-08
33903|Bamboo Springs pluton|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2950 Ma||||||07-NOV-08
38817|Banded Schist, Lower|23927|4|Described|p52||Archean|Informal name - local name in the Yilgarn Star gold deposit area.  Geological Province: Yilgarn Craton.||||||07-NOV-08
40811|Bangemall 'Group'|50188|6|Mentioned|p9, 12|Mesoproterozoic|Mesoproterozoic|Informal name. Upgraded to Bangemall Supergroup.||||||14-JUL-04
24690|Bangemall Beds|36884|6|Mentioned|p147|||Renamed Bangemall Group.||||||
24690|Bangemall Beds|39210|5|Briefly described|p44|||||||||
24690|Bangemall Beds|42260|6|Mentioned|p3|||||||||
27106|Bangemall Group|12099|5|Briefly described|p676, p677 Fig.2, p681, p684 Fig.8|Statherian|Statherian||~1640 Ma.|||Unconformably overlies Ravelstone Formation.||04-MAR-13
27106|Bangemall Group|22478|6|Mentioned|p23||Mesoproterozoic|Bangemall Basin||||||
27106|Bangemall Group|22491|5|Briefly described|p 9|||Yilgarn Craton||||||
27106|Bangemall Group|22501|6|Mentioned|p117|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|22589|6|Mentioned|p123|Neoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|22660|5|Briefly described|p 304|||||||||
27106|Bangemall Group|22694|5|Briefly described|p8|||Bangemall Basin||||||
27106|Bangemall Group|22695|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|22696|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|22697|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|22698|5|Briefly described|map|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|22716|5|Briefly described|table4, p236|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Savory Bub-Basin||||||
27106|Bangemall Group|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
27106|Bangemall Group|22905|5|Briefly described|p51-52|Mesoproterozoic|Mesoproterozoic|Superseded by Bangemall Supergroup.  Age 1.64+/-1.00 Ga||||||24-JAN-06
27106|Bangemall Group|22907|6|Mentioned|39|||||||||
27106|Bangemall Group|22940|4|Described|p20, Fig.6 p14, Fig.1 p3|Mesoproterozoic|Mesoproterozoic|of Bangemall Basin.||||||
27106|Bangemall Group|23152|5|Briefly described|p71|||||||||
27106|Bangemall Group|23156|4|Described|p8|Mesoproterozoic|Mesoproterozoic|First Edition of BULLEN showed the Bangemall Group of the Bangemall Basin occupying about 99% of the sheet.  This area has been reduced to about 14% following the recognition of the Late Proterozoic Savory Basin.  Mafic Sills and irregular bodies intrude||||||
27106|Bangemall Group|23280|5|Briefly described|p1084-5||Statherian|Max Age: ~1640 Ma.||||||
27106|Bangemall Group|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|23325|5|Briefly described|map legend|Precambrian|Precambrian|||||||
27106|Bangemall Group|23403|6|Mentioned|p3|||Superseded by Bangemall Supergroup.||||||
27106|Bangemall Group|23485|6|Mentioned|p30|||Superseded by Bangemall Supergroup.||||||
27106|Bangemall Group|23570|5|Briefly described|p14|||Geological Province: Pilbara Craton||||||
27106|Bangemall Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlying unit Bresnahan Group.||||||
27106|Bangemall Group|23589|5|Briefly described|p6, table 6|||1638+/-14 Ma (SHRIMP U-Pb zircon of Coobarra Formation). Underlying unit Earaheedy Group.||||||
27106|Bangemall Group|23592|5|Briefly described|p2 Fig 1|Mesoproterozoic|Mesoproterozoic|Age: 1.65 Ga. Underlying unit Padbury Group. Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23594|5|Briefly described|p9 Fig. 6|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23597|5|Briefly described|p11|Statherian|Statherian|||||||
27106|Bangemall Group|23602|6|Mentioned|p5|||||||||
27106|Bangemall Group|23723|5|Briefly described|p1|Proterozoic|Proterozoic|See also page 5. Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23724|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|23725|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|23744|4|Described|p24|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|23746|5|Briefly described|p8 Fig 5|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|23747|5|Briefly described|p16|||Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23749|4|Described|p14|Proterozoic|Proterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|23760|6|Mentioned|p5|||||||||
27106|Bangemall Group|24017|6|Mentioned|p21|||Superseded by Bangemall Supergroup.||||||
27106|Bangemall Group|24018|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|24114|6|Mentioned|p8|||||||||
27106|Bangemall Group|24183|5|Briefly described|p1, p5|Mesoproterozoic|Mesoproterozoic|Superseded by the Bangemall Supergroup. Contains the Cornelia Sandstone and Scorpion Subgroup (Williams 1990).||||||
27106|Bangemall Group|24203|5|Briefly described|p297|Proterozoic|Proterozoic|Age: <1640 Ma.  Geological Province Carnarvon Basin.||||||
27106|Bangemall Group|24531|6|Mentioned|p36|||||||||
27106|Bangemall Group|24535|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of Muhling and Brakel (1985) Included Kahrban Subgroup. See Bangemall Supergroup.||||||26-NOV-13
27106|Bangemall Group|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Superseded by Bangemall Supergroup.||||||
27106|Bangemall Group|29596|6|Mentioned|Table 1|||||||||
27106|Bangemall Group|29845|6|Mentioned|p159|||||||||
27106|Bangemall Group|29846|6|Mentioned|p103|||||||||
27106|Bangemall Group|29847|6|Mentioned|p73|||||||||
27106|Bangemall Group|29848|6|Mentioned|p414|||||||||
27106|Bangemall Group|29850|6|Mentioned|p1020|||||||||
27106|Bangemall Group|29916|6|Mentioned|p114|||||||||
27106|Bangemall Group|30010|6|Mentioned|p43|||||||||
27106|Bangemall Group|30354|6|Mentioned|p9|||Palaeogeography||||||
27106|Bangemall Group|30363|6|Mentioned|p6|||||||||
27106|Bangemall Group|30482|6|Mentioned|p170|||||||||
27106|Bangemall Group|30484|6|Mentioned|Fig.29|||||||||
27106|Bangemall Group|30503|6|Mentioned|Table 1|||||||||
27106|Bangemall Group|30704|5|Briefly described|p59|||||||||
27106|Bangemall Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
27106|Bangemall Group|30880|6|Mentioned|p528|||||||||
27106|Bangemall Group|30881|4|Described|p525|||||||||
27106|Bangemall Group|30884|5|Briefly described|p156|||||||||
27106|Bangemall Group|31217|6|Mentioned|p42|||Mention P40.||||||
27106|Bangemall Group|31393|6|Mentioned|Pl.25|||M. Proterozoic||||||
27106|Bangemall Group|31670|6|Mentioned|p911|||||||||
27106|Bangemall Group|31828|6|Mentioned|p37|||Proterozoic on map. See also asbestos P41.||||||
27106|Bangemall Group|31854|6|Mentioned|p65|||||||||
27106|Bangemall Group|31914|6|Mentioned|p95|||||||||
27106|Bangemall Group|31940|6|Mentioned|p5|||Middle Proterozoic. Fig.1||||||
27106|Bangemall Group|32586|6|Mentioned|p113|||||||||
27106|Bangemall Group|32720|6|Mentioned|p8|||1080 + or - 80 my. mid. Riphean Correlation||||||
27106|Bangemall Group|32722|6|Mentioned|Fig.3|||Stromatolite||||||
27106|Bangemall Group|32727|6|Mentioned|p7|||||||||
27106|Bangemall Group|32954|6|Mentioned|p184|||||||||
27106|Bangemall Group|32972|5|Briefly described|p64|||Calcretes. Middle Proterozoic||||||
27106|Bangemall Group|32974|6|Mentioned|p23|||||||||
27106|Bangemall Group|33536|3|Fully described|p84|||Precambian. 1000my approx||||||
27106|Bangemall Group|33539|6|Mentioned|p92|||Correlation||||||
27106|Bangemall Group|33542|6|Mentioned|p411|||||||||
27106|Bangemall Group|33544|5|Briefly described|p30|||See also P31. Age||||||
27106|Bangemall Group|33630|6|Mentioned|p908|||||||||
27106|Bangemall Group|33849|4|Described|p126|||||||||
27106|Bangemall Group|34066|5|Briefly described|p10|||Mid.-Prot.  See also P11||||||
27106|Bangemall Group|34115|6|Mentioned|Fig.|||Map legend||||||
27106|Bangemall Group|34124|4|Described|Table 1|||Lower Proterozoic. see also PP3-17||||||
27106|Bangemall Group|34135|4|Described|Table 2|||Middle Proterozoic. See also PP6,7,14,17.||||||
27106|Bangemall Group|34202|6|Mentioned|p1056|||See also P1058||||||
27106|Bangemall Group|34287|6|Mentioned|p37|||||||||
27106|Bangemall Group|34702|6|Mentioned|p31|||||||||
27106|Bangemall Group|34999|6|Mentioned|Table 17|||||||||
27106|Bangemall Group|35052|6|Mentioned|p18|||||||||
27106|Bangemall Group|35260|6|Mentioned|p5|||Map legend||||||
27106|Bangemall Group|35269|6|Mentioned|p295|||||||||
27106|Bangemall Group|35596|4|Described|p7|||||||||
27106|Bangemall Group|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|35902|6|Mentioned|p7|||||||||
27106|Bangemall Group|35949|6|Mentioned|Fig.8|||||||||
27106|Bangemall Group|35975|6|Mentioned|p104|||||||||
27106|Bangemall Group|35976|6|Mentioned|p107|||||||||
27106|Bangemall Group|35982|6|Mentioned|p136|||||||||
27106|Bangemall Group|36003|5|Briefly described|p1027|||||||||
27106|Bangemall Group|36257|6|Mentioned|p29|||||||||
27106|Bangemall Group|36258|6|Mentioned|p49|||||||||
27106|Bangemall Group|36551|6|Mentioned|p101|||||||||
27106|Bangemall Group|36870|6|Mentioned|p60|||||||||
27106|Bangemall Group|36880|3|Fully described|p110|||||||||
27106|Bangemall Group|36881|6|Mentioned|p117|||||||||
27106|Bangemall Group|36882|6|Mentioned|p120|||||||||
27106|Bangemall Group|36883|6|Mentioned|p143|||||||||
27106|Bangemall Group|36884|3|Fully described|p147|||Formerly Bangemall Beds and Bangemall Series.||||||
27106|Bangemall Group|36891|6|Mentioned|p442|||||||||
27106|Bangemall Group|37018|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|37020|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|37022|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|37023|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|37024|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|37026|4|Described|p3|||||||||
27106|Bangemall Group|37212|4|Described|p14|||||||||
27106|Bangemall Group|37213|4|Described|p21|||||||||
27106|Bangemall Group|37214|4|Described|p8|||||||||
27106|Bangemall Group|37299|6|Mentioned|Fig.1|||||||||
27106|Bangemall Group|37328|6|Mentioned|p4|||||||||
27106|Bangemall Group|37371|6|Mentioned|p377|||||||||
27106|Bangemall Group|37422|6|Mentioned|Fig.1|||||||||
27106|Bangemall Group|37577|6|Mentioned|p6|||||||||
27106|Bangemall Group|37643|5|Briefly described|p5.5.3|||||||||
27106|Bangemall Group|37707|6|Mentioned|p14|||||||||
27106|Bangemall Group|38243|6|Mentioned|Fig.2|||||||||
27106|Bangemall Group|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|38299|4|Described|p7|||||||||
27106|Bangemall Group|38493|4|Described|p31|||||||||
27106|Bangemall Group|38515|4|Described|p15|||||||||
27106|Bangemall Group|38516|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|38768|6|Mentioned|p81|||||||||
27106|Bangemall Group|38978|6|Mentioned|p132|||||||||
27106|Bangemall Group|38988|6|Mentioned|p6|||See also P8||||||
27106|Bangemall Group|39128|6|Mentioned|p174|||||||||
27106|Bangemall Group|39162|6|Mentioned|Fig.24|||||||||
27106|Bangemall Group|39168|5|Briefly described|p71|||Age||||||
27106|Bangemall Group|39171|5|Briefly described|p80|||||||||
27106|Bangemall Group|39210|3|Fully described|p44|||||||||
27106|Bangemall Group|39370|6|Mentioned|p3|||||||||
27106|Bangemall Group|39424|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|39426|4|Described|p12|||See also P13||||||
27106|Bangemall Group|39427|6|Mentioned|p4|||||||||
27106|Bangemall Group|39558|6|Mentioned|p260|||See also Table 1||||||
27106|Bangemall Group|39697|5|Briefly described|p130|||||||||
27106|Bangemall Group|39894|6|Mentioned|p47|||||||||
27106|Bangemall Group|40088|6|Mentioned|p228|||||||||
27106|Bangemall Group|40089|2|Defined|p17|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|40105|6|Mentioned|p311|||||||||
27106|Bangemall Group|40303|6|Mentioned|p31|||||||||
27106|Bangemall Group|40340|6|Mentioned|p7|||||||||
27106|Bangemall Group|40347|6|Mentioned|p20|||||||||
27106|Bangemall Group|40354|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|40355|4|Described|p11|||||||||
27106|Bangemall Group|40369|6|Mentioned|Fig.1|||||||||
27106|Bangemall Group|40554|6|Mentioned|p29|||||||||
27106|Bangemall Group|40888|6|Mentioned|p153|||||||||
27106|Bangemall Group|40899|6|Mentioned|p22|||||||||
27106|Bangemall Group|40900|4|Described|p33|||||||||
27106|Bangemall Group|40904|6|Mentioned|p85|||||||||
27106|Bangemall Group|40909|6|Mentioned|p22|||||||||
27106|Bangemall Group|40934|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27106|Bangemall Group|40936|6|Mentioned|Map legend|||||||||
27106|Bangemall Group|40937|3|Fully described|p5|||||||||
27106|Bangemall Group|40938|6|Mentioned|p2|||||||||
27106|Bangemall Group|40989|4|Described|p32|||||||||
27106|Bangemall Group|41144|5|Briefly described|p807|||||||||
27106|Bangemall Group|41277|6|Mentioned|p84|||||||||
27106|Bangemall Group|41360|6|Mentioned|p191|||||||||
27106|Bangemall Group|41669|6|Mentioned|p36|||||||||
27106|Bangemall Group|41768|5|Briefly described|p36|||||||||
27106|Bangemall Group|41844|6|Mentioned|p72|||||||||
27106|Bangemall Group|41955|6|Mentioned|Fig.1 P4|||||||||
27106|Bangemall Group|42013|5|Briefly described|Map Legend|Proterozoic||||||||
27106|Bangemall Group|42020|6|Mentioned|Fig.1 P317|||||||||
27106|Bangemall Group|42112|4|Described|p15|||See also Fig.1||||||
27106|Bangemall Group|42148|6|Mentioned|p693|||||||||
27106|Bangemall Group|42260|6|Mentioned|p3|||||||||
27106|Bangemall Group|42278|6|Mentioned|p33|||||||||
27106|Bangemall Group|42435|6|Mentioned|p46|||||||||
27106|Bangemall Group|42471|4|Described|p19|||Bangemall Basin.||||||
27106|Bangemall Group|42704|5|Briefly described|Plate 2E|Mesoproterozoic|Mesoproterozoic|Age: c. 1600Ma.  Lithology includes sandstone, siltstone, shale, conglomerate, dolomite, chert. Intruded by dolerite sills.||||||07-AUG-08
27106|Bangemall Group|42708|5|Briefly described|Plate 1|Proterozoic||||||||
27106|Bangemall Group|42730|5|Briefly described|Fig 12, P15|||||||||
27106|Bangemall Group|43055|6|Mentioned|p20|||||||||
27106|Bangemall Group|43069|6|Mentioned|p26|||||||||
27106|Bangemall Group|43209|5|Briefly described|map legend||Mesoproterozoic|||||||
27106|Bangemall Group|43210|5|Briefly described|Fig.1 p2,p7.|Neoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|43229|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27106|Bangemall Group|43238|5|Briefly described|p7|||||||||
27106|Bangemall Group|43255|5|Briefly described|map legend||Proterozoic|||||||
27106|Bangemall Group|43256|4|Described|5-21||Proterozoic|||||||24-NOV-09
27106|Bangemall Group|43348|6|Mentioned|p1|||||||||
27106|Bangemall Group|43492|4|Described|8|||||||||
27106|Bangemall Group|43595|6|Mentioned|Fig 3-43,p348,444|||Age: 1.0-1.1 Ga||||||
27106|Bangemall Group|43756|6|Mentioned|p533|||||||||
27106|Bangemall Group|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27106|Bangemall Group|43831|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27106|Bangemall Group|44111|6|Mentioned|p.56 Fig. 1, p61 Fig.3|||||||||
27106|Bangemall Group|44139|6|Mentioned|p277-278|||Blockley and de la Hunty (1975). Included rocks now assigned to the Yeneena Group after a basal unconformity was found below the Calyie Sandstone of the Collier Subgroup (Bangemall Group). Yet further complications in the regional stratigraphy are discussed.||||||
27106|Bangemall Group|44141|6|Mentioned|p304-307||||1.5 Ga (Williams).|||Overlies Bresnahan Group.||
27106|Bangemall Group|44142|5|Briefly described|p308-329|||Of Daniels (1975); formerly "Bangemall Beds" or "Bangemall Series" of Maitland (1909). Subsequently modified by Muhling and Brakel (1976, 1985) and Chuck (1984). Stratigraphic schemas compared. Outcrops over 17,000 km2. Markedly older age determinations discussed.|c.1.1 Ga.||Includes Edmund, Mucalana, Collier, Manganese, Scorpion and Kahrban Subgroups and Cornelia Sandstone.||A thick sequence of mainly clastic sedimentary rocks.|13-MAR-18
27106|Bangemall Group|44151|6|Mentioned|p158, p160 Fig.2-146, p163||||||Includes Manganese Subgroup.|||
27106|Bangemall Group|44152|6|Mentioned|p176 Fig.2-154|||||||||
27106|Bangemall Group|44319|14|Not recorded|map legend||Mesoproterozoic|M.Proterozoic inc. Kurabuka Fm. Fords Ck.Sh., Coodardoo Fm., Curran Fm., Ullawarra Fm., Devil Creek Fm. Discovery Chert, Kiangi Ck Fm., Irregully Fm.||||||
27106|Bangemall Group|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
27106|Bangemall Group|44831|5|Briefly described|Map Legend||Proterozoic|||||||
27106|Bangemall Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27106|Bangemall Group|45149|6|Mentioned|p18|||||||||
27106|Bangemall Group|46917|6|Mentioned|p172|||||||||
27106|Bangemall Group|49895|6|Mentioned|p5|||||||||
27106|Bangemall Group|49896|6|Mentioned|p4 Fig. 1, p6|||Unconformably overlies the Padbury Group. See also p12 Fig. 8, p13.||||||
27106|Bangemall Group|50221|5|Briefly described|p296 Fig.1|Mesoproterozoic|Mesoproterozoic|Possibly misspelt - intended to be Bangemall Supergroup? Age: <1640 Ma.||||||
27106|Bangemall Group|50222|5|Briefly described|p325|Mesoproterozoic|Mesoproterozoic|Unconformably overlies Ravelstone Formation.||||||
27106|Bangemall Group|50224|5|Briefly described|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Mulgarra Sandstone (Minningarra Subgroup).||||||07-FEB-11
27106|Bangemall Group|50225|6|Mentioned|p385, p386|Mesoproterozoic|Mesoproterozoic|Superseded by Bangemall Supergroup.  See also p387 Fig. 2, p390.||||||07-FEB-11
27106|Bangemall Group|50425|6|Mentioned|p2.2|||Overlies: Mount Danvers Granodiorite (unconformably).||||||10-AUG-04
27106|Bangemall Group|50626|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin.||||||
27106|Bangemall Group|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|Sedimentary rocks.||||||07-FEB-11
27106|Bangemall Group|61269|6|Mentioned|p86 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|62289|6|Mentioned|plate 1 (area of this map), p4|||Geol. Prov: Bangemall Basin.||||||
27106|Bangemall Group|62428|5|Briefly described|p336, p346|||Includes the Irregully Formation in the lower section.||||||10-FEB-09
27106|Bangemall Group|63869|6|Mentioned|p2, p27, p39, p51, p53|||Formerly Bangemall Series, series, Beds and beds [all of which appear in Maitland, 1909]. Stratigraphy of the Group appeared in Halligan and Daniels (1964) p88. Subsequently Bangemall Supergroup.||||||
27106|Bangemall Group|64329|5|Briefly described|p15|Proterozoic|Proterozoic|Intruded by the Yangibana ironstone dykes.||||||
27106|Bangemall Group|64384|5|Briefly described|p5, p48 Fig. 40|Neoproterozoic|Neoproterozoic|Unconformably overlies the Sylvania Inlier outcrops.||||||07-FEB-11
27106|Bangemall Group|64772|6|Mentioned|p5,p13|||Described by Muhling and Brakel (1985) but now superseded by Bangemall Supergroup when Bangemall Basin stratigraphy was reviewed (Martin et al (1999). .||||||25-NOV-13
27106|Bangemall Group|64777|5|Briefly described|p1|||Obsolete name. Blockley and de la Hunty (1975) assigned units in Tarcunyah Group to this unit, which was subsequently elevated to Supergroup status by Martin et al. (1999).||||||
27106|Bangemall Group|64943|6|Mentioned|p27 Table 5|||Includes Manganese Subgroup||||||
27106|Bangemall Group|65008|6|Mentioned|p24|||Of Tyler (1991).||||||06-APR-16
27106|Bangemall Group|65102|6|Mentioned|p363, Figure 4-38|Mesoproterozoic|Mesoproterozoic|Bangemall and Savory Basins.||||||
27106|Bangemall Group|65403|6|Mentioned|p14.||||||Includes Manganese Subgroup.|||
27106|Bangemall Group|65404|6|Mentioned|p244, p245 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|65408|5|Briefly described|p82, p84 Fig.1, 85|Mesoproterozoic|Statherian|Deposited on a basement of deformed, uplifted and eroded rocks of the Capricorn Orogeny after c.1650 Ma. Displaced by the Jenkin Fault. Age is of felsic volcanics low in Group.|SHRIMP U/Pb zircon 1638 +/- 14 Ma, Coobarra Fm||Includes Coobarra Formation.||Includes felsic volcanic rocks.|01-FEB-12
27106|Bangemall Group|65411|6|Mentioned|p89 Fig.1.|||||||||
27106|Bangemall Group|65412|6|Mentioned|p97 Fig.1.|||||||||
27106|Bangemall Group|65416|6|Mentioned|p139 Fig.4.|Mesoproterozoic|Mesoproterozoic|||||Is overlain unconformably by Browne Formation.||
27106|Bangemall Group|65419|5|Briefly described|p4 Fig.1, p29, p37, p42, p50.|Mesoproterozoic|Mesoproterozoic|A flat-lying quartz-pebble conglomerate at the base of this unit unconformably overlies the Labouchere Formation.|1.6 Ga (Nelson, 1995).|||Unconformably overlies Bryah and Padbury Groups.||
27106|Bangemall Group|65829|6|Mentioned|p27.|||Superseded.||Included Waltha Woora Formation and Woblegun Formation.||||
27106|Bangemall Group|65830|6|Mentioned|p14|||Replaced by the Bangemall Supergroup.||||||
27106|Bangemall Group|66217|6|Mentioned|p55.|||Bangemall Basin. Is older than the Mundine Well Dolerite Suite.||||||
27106|Bangemall Group|67127|5|Briefly described|p89|Palaeoproterozoic|Palaeoproterozoic|Capricorn Orogen. Hosts a carbonatite REE deposit called the Yangibana 'ironstones' prospect.|||||Sedimentary rocks.|
27106|Bangemall Group|67130|6|Mentioned|p3 fig 2||||c. 1640 Ma|||Unconformably overlies Wyloo Group, Ashburton Formation||
27106|Bangemall Group|67855|5|Briefly described|p201, 208, 211,212, 221,222,223,224,230|Mesoproterozoic|Mesoproterozoic|Bangemall Basin.|1.6-1.0 Ga|||||
27106|Bangemall Group|68035|5|Briefly described|p292 Fig 6|Statharian|Statherian||~1640 Ma|||Unconformably overlies Wyloo Group.||
27106|Bangemall Group|68280|6|Mentioned|p5||||c. 1640 Ma||||Sandstone and siltstone.|
27106|Bangemall Group|68561|5|Briefly described|2_5M_GEOLOGYP98_LUT|Mesoproterozoic|Mesoproterozoic|[Old name] used in 2_5M_GEOLOGYP98_LUT. [Replaced by Bangemall Supergroup].||||||
27106|Bangemall Group|69166|6|Mentioned|91591.1.pdf|Paleoproterozoic|Paleoproterozoic|||Bangemall Supergroup|Includes Coobarra Formation|||
27106|Bangemall Group|69745|6|Mentioned|p269|||Hamersley Province.||||Unconformably overlies Bresnahan Group.||
27106|Bangemall Group|70804|5|Briefly described|p4, p16, p21, p33, p37-p38|||||||Unconformably overlies the Ravelstone Formation and the Millidie Creek Formation.||
27106|Bangemall Group|70958|6|Mentioned|p1, p13, Fig. 1|||Predominantly sedimentary rocks. Younger than Paleoproterozoic.||||Overlaps [overlies?] Wandarry Shale Member, Ashburton Formation.||
27106|Bangemall Group|71003|6|Mentioned|p74|||Pilbara Craton. Contains the [probably superseded] Collier Subgroup. Obsolete; see the Bangemall Supergroup.||||||
27106|Bangemall Group|71786|6|Mentioned|p92|Mesoproterozoic|Mesoproterozoic|||||||
27106|Bangemall Group|72758|4|Described|p50-54, p7-9 Tb.1, p30, p37, p48.|Mesoproterozoic|Mesoproterozoic|Established by Halligan and Daniels (1964). Divided into 8 formations. Only the lower two occur in the Wyloo sheet area. Bangemall Group rocks, and older rocks are cut by dolerite dykes generally less than 10 m, but some over 100 m thick. See also p4 Fig.1, p57.|c. 1100 Ma by Rb/Sr methods||Includes Irregully Formation and Kiangi Creek Formation.|Unconformably overlies Mount Minnie Group, Morrissey Metamorphic Suite, ?Wongida Creek Granodiorite.|Includes felsic rocks.|
38127|Bangemall Group""|23525|6|Mentioned|p28|||Superseded by Bangemall Supergroup.   Geological Province: Bangemall Basin||||||
38127|Bangemall Group""|24017|6|Mentioned|p21|||||||||
38127|Bangemall Group""|50008|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Superseded. Elevated to Supergroup status by Martin et al., 1999.||||||
38127|Bangemall Group""|50188|6|Mentioned|p16|||Upgraded to Bangemall Supergroup.  Informal name.||||||
72702|Bangemall Supergroup Sills|62869|5|Briefly described|p627|Mesoproterozoic|Mesoproterozoic|Informal name referring to sills within the Bangemall Supergroup.  Of Wingate et al (2002) and abbreviated to BSS. Age: 1070+/-6Ma. Geological Province: Bangemall Basin.||||||22-NOV-06
40810|Bangemall Supergroup, Lower|50188|5|Briefly described|p10 Fig. 3.|Paleoproterozoic|Paleoproterozoic|Informal name.  Age: ~1640Ma.||||||07-NOV-08
40810|Bangemall Supergroup, Lower|64283|5|Briefly described|p50 Fig. 1, p53|||Informal - see Bangemall Supergroup.||||||07-FEB-11
40813|Bangemall Supergroup, Upper|50188|5|Briefly described|p10 Fig. 3|Mesoproterozoic|Mesoproterozoic|Informal name.  Age: ~1200Ma.||||||16-JUL-08
40813|Bangemall Supergroup, Upper|64283|5|Briefly described|p50 Fig. 1, p53|||Informal - see Bangemall Supergroup. Includes the Collier Group.||||||07-FEB-11
69022|Bapinmarra dolerite|60976|6|Mentioned|p12|||Informal name - see Bapinamarra Dolerite. Contains minor granophyre. Associated with the Bronzewing fold deposit / Bronzewing anticline. Geological Province: Yilgarn Craton.||||||
69022|Bapinmarra dolerite|60978|6|Mentioned|p56, p62|||Associated with the Bronzewing gold deposit. Geological Province: Yilgarn Craton. See also p68 Fig.3.||||||
69022|Bapinmarra dolerite|60980|5|Briefly described|p142 Fig.2, p145|||Informal name.||||||
38081|Baramine Member|23570|5|Briefly described|p231 Appendix 1|||Abbreviation by authors of  Baramine Volcanic Member of Hickman et al. (1983).||||||
38081|Baramine Member|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Jeerinah Formation. Basalt and basaltic andesite, and basaltic, volcanic sandstone and siltsone; local accretionary lapilli. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
38081|Baramine Member|65829|4|Described|p15, pp21-22.|||Formerly the Baramine Volcanic Member (Hickman 1983); redefined by Williams and Trendall (1998c). Thick lenticular bodies of mafic volcanics; thickness varies from 100 to 250 m. The volcaniclastic component appears to be a mixture of resedimented syneruptive volcaniclastic deposits and volcanogenic sedimentary deposits.||Unit in Jeerinah Formation.|||Massive, amygdaloidal and vesicular dark grey to grey-green basalt and basaltic andesite, interlayered with basaltic volcanic sandstone and siltstone, and local accretionary lapilli beds; local pillow basalt; interbedded silicified mudstone.|
38081|Baramine Member|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Jeerinah Formation|||Basalt and basaltic andesite, and basaltic volcanic sandstone and siltstone; local accretionary lapilli. Coarse to fine grained basaltic volcaniclastic rocks with local accretionary lapilli; thin basalt flows.|
29304|Barbwire Formation|33519|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
29304|Barbwire Formation|36225|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||05-FEB-20
29304|Barbwire Formation|36634|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|||||||
29304|Barbwire Formation|38878|6|Mentioned|Map legend|Tithonian|Kimmeridgian|Oxfordian - Tithonian||||||
29304|Barbwire Formation|41356|6|Mentioned|Fig.45|||||||||
29304|Barbwire Formation|45153|2|Defined|App.6-108|Late Jurassic|Late Jurassic|See also App.4-74||||||
29304|Barbwire Formation|66949|6|Mentioned|p67 Appx.5|Jurassic|Jurassic|Mentioned in discussion of Barbwire 1 well.||||||
80318|Bardwine Sandstone|67202|5|Briefly described|p69-71|Late Jurassic|Late Jurassic|Fluvial deposits.|||||Fine- to coarse-grained sandstone, conglomerate, minor siltstone.|
42354|Barimunya Member, Upper|60539|6|Mentioned|p502|||||||||
79802|Barloweerie gabbro|70419|6|Mentioned|p8|Neoarchean|Neoarchean||2711 Ma.|Yalgowra Suite.||||
82117|Barrabiddy Formation|72910|6|Mentioned|p40|||Of previoius authors. Now included in Callytharra Formation.||||||
69194|Barrack Point gneiss|24542|5|Briefly described|p7|Neoproterozoic|Mesoproterozoic|Not intended as a formal name. Massive brown rock. Of Leeuwin Complex.||||||
75541|Barrambie Intrusion|65271|5|Briefly described|Map legend|Archean|Archean|Metamorphosed medium to coarse-grained layered mafic rock, typically deeply weathered. Of Barrambie greenstone belt, Murchison Granite-Greenstone Terrane, Yilgarn Craton.||||||10-DEC-09
75541|Barrambie Intrusion|65897|5|Briefly described|Map legend|Neoarchean|Neoarchean|Medium- to coarse-grained, layered mafic rock; metamorphosed; typically deeply weathered. Unit in Barrambie greenstone belt, Youanmi Terrane, Yilgarn Craton.||||||
39909|Barramine Volcanic Member|24353|5|Briefly described|p6|Archean|Archean|Misspelt - see Baramine Volcanic Member. Parent: Jeerinah Formation. Geological Province: Pilbara Craton||||||07-NOV-08
67852|Barrett Well banded gneiss|60076|6|Mentioned|p24|Archean|Archean|Informal reference to banded gneiss in the Barrett Well region - not intended as a formal name.  Quartzo-feldspathic rocks.  Age: 2675+/-2Ma.||||||07-NOV-08
28351|Barrow Formation""|41440|5|Briefly described|p137|||||||||
42337|Barrow Group Sandstones|24315|5|Briefly described|p43|Early Cretaceous|Early Cretaceous|Informal - see Barrow Group. Geological Province: Barrow Sub-Basin.||||||07-DEC-04
40317|Barrow Group, middle|50024|5|Briefly described|p13||Cretaceous|Informal name.  Contains the B. reticulatum sand.  Geological Province: Carnarvon Basin.||||||
68130|Barrow Group, upper|24315|6|Mentioned|p43|Early Cretaceous|Early Cretaceous|Informal - refer to Barrow Group. Geological Province: Barrow Sub-Basin||||||
83344|Barry Formation|73391|6|Mentioned|Appendices.|||Mentioned in Field Data Appendix. described as: finely bedded quartz sandstone; Barry Formation (Ballarat Turbidite, with poorly exposed Ballarat Conglomerate to the north of here.||||||22-JUN-22
38806|Barton dolerite|23931|6|Mentioned|p201 Table 1|||Informal name - see Barton Dolerite. Geological Province: Yilgarn Craton.||||||
38806|Barton dolerite|60978|6|Mentioned|p68 Fig.3|||Informal reference to a dolerite at the Jundee gold deposit. Geological Province: Yilgarn Craton.||||||
35376|Basal Pegmatite|23904|5|Briefly described|p26 Fig.2(b), p34 Fig.5|||Informal name. Geological Province: Yilgarn Craton.||||||
42399|Bassendean Dune System|23816|6|Mentioned|p255|Late Pleistocene|Middle Pleistocene|Superseded by the Bassendean Sand (Playford and Low, 1972). Geological Province: Perth Basin.||||||16-DEC-04
42399|Bassendean Dune System|63745|6|Mentioned|p59, p67|||See also p60 Fig. 1.||||||07-FEB-11
42399|Bassendean Dune System|69840|6|Mentioned|p183|Pleistocene|Neogene|Also termed Bassendean Sand. Parallel to the coast this unit is the most easterly and oldest of three associated dune systems (Quindalup Dune System and Spearwood Dune System.|||||Quartz sand.|
42399|Bassendean Dune System|71780|14|Not recorded|p51 Table 1, Plate 2||Quaternary|No white card.||||||
73387|Bassendean Dunes|60556|5|Briefly described|p21||Informal|||||||
73387|Bassendean Dunes|63330|5|Briefly described|p192, p193 Fig. 5, p194|Quaternary|Quaternary|This term is more a structural name than a stratigraphic unit - relating directly to Bassendean Sand beneath it. Undulating terrain mostly of low degraded dunes and interdune flats and basins. In Perth Basin/Swan Coastal Plain.||||||05-JUN-07
79239|Bassendean Sandstone|70097|5|Briefly described|p19 Fig.3, p20 Fig.4|Pleistocene|Pliocene|Perth Basin. Beermullah Trough, Mandurah Terrace and Dandaragan Trough.||||Overlies Yoganup, Ascot Formations.|?Sandstone.|30-SEP-16
79239|Bassendean Sandstone|71377|5|Briefly described|p7|Quaternary|Neogene|Mandurah Terrace, Perth Basin.||||||
32962|Bassendean System""|44303|14|Not recorded|p.12|||ref. to McArthur & Bettenay 196-, Welch 1964 (I/50-5,9).||||||
28353|Bassendean sand|31912|6|Mentioned|p54|||P55||||||
28353|Bassendean sand|33747|5|Briefly described|p1083|||||||||
28353|Bassendean sand|39554|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
28353|Bassendean sand|40086|6|Mentioned|p96|||||||||
38775|Beasley Quartzite|23890|5|Briefly described|p5 Fig.2|||Geological Province: Ashburton Basin.||||||
38775|Beasley Quartzite|69745|6|Mentioned|p270, 286|||Hamersley Province. See also references to Beasley River Quartzite (p271, 273, 275, 287).||Lower Wyloo Group.||||
73758|Beasley River "Limonites"|63432|5|Briefly described|p734|||Informal name. Geological Province: Hamersley Province. Channel iron deposit.||||||07-FEB-11
24704|Beasley River Quartzite""|35976|6|Mentioned|p107|||Used in pre-revision sense.||||||
24704|Beasley River Quartzite""|41846|6|Mentioned|Fig.1|||||||||
38997|Beasley river pillow basalts|23870|6|Mentioned|p229 Fig.3|||Informal name.||||||
29961|Beaton Creek Conglomerate""|43055|6|Mentioned|Table 1|||refers to de la Hunty (1964).||||||
32637|Beaton's Creek Conglomerate|45923|4|Described|p82-85||Neoproterozoic|On many pages: 67,86,102,135,136. Map SF51-5. Named from their largest development in the Beaton¿s Creek locality, north-westerly of Nullagine township. (Ref. 299269).||||||03-FEB-17
34332|Beaton's Creek Conglomerate Member|22717|6|Mentioned|p21|||||||||03-FEB-17
34332|Beaton's Creek Conglomerate Member|39426|6|Mentioned|p10|Proterozoic|Proterozoic|Is a local member of Hardey Sandstone. In the past an important source of gold at Nullagine.||||||
38757|Beatons Creek Member|24025|5|Briefly described|p33|||Of Hardey Formation.  Geological Province: Pilbara Craton.||||||
81548|Beattie Park Member|71484|6|Mentioned|p138|||Geological province: Of Padbury Basin. Misspelt; see Beatty Park Member.||||||30-AUG-19
41200|Beatty Park member|50222|6|Mentioned|p327|||Informal - see Beatty Park Member.||||||
70568|Becher Sand Unit|61521|6|Mentioned|p39|||Informal name of Semeniuk and Searle (1985) - see Becher Sand. Combined carbonate sand and muddy sand facies.||||||
35635|Beckett Limestone Member|23279|6|Mentioned|p12|||||||||
35635|Beckett Limestone Member|44144|6|Mentioned|p508 Tb.4-21|Sakmarian|Sakmarian|||Holmwood Shale|||Fossiliferous limestone.|
81884|Bee Gorge Formation|72569|6|Mentioned|p2|||Of the Hamersley Basin. Appears also as the Bee Gorge Member on p2.|||||Crystal rich tuff.|
29955|Bee Hill Sandstone""|43055|6|Mentioned|p21|||refers to de la Hunty (1963).||||||
29955|Bee Hill Sandstone""|44142|6|Mentioned|p316 Tb.4-4|||de la Hunty (1963). Included in Coondoon Formation.||||||
24707|Beegagong Claystone|42123|6|Mentioned|p50|||Misspelling of Beedagong?||||||
75817|Beekeeper Member|5257|6|Mentioned|p153|Late Permian|Artinskian|Of Wagina Formation, Perth Basin. Tupper et al. (1994) revision of Hall and Kneale (1992) definition of Beekeeper Formation. Includes brachiopods with a preferred age of Ufimian (early late Permian). These rocks formerly included in Carynginia Formation.||||||
83183|Beenong dykes|73056|6|Mentioned|p293|||Yilgarn Craton, southeast. NW-trending dykes, undated but likely less than 1140 Ma.||||||
83183|Beenong dykes|73057|6|Mentioned|p4|||Yilgarn Craton, southeast. Undated but likely less than 1140 Ma. NW-trending dykes.||||||
69385|Beete hornblende gabbro|60979|6|Mentioned|p96 Fig.5|||Informal name. Geological Province: Yilgarn Craton.||||||
34582|Bejah claystone|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
34582|Bejah claystone|72497|5|Briefly described|p3 Fig.2.|Albian|Aptian|Shown, along with Anketell Formation, as occuring in the Anketell Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform.||||Laterally equivalent to Anketell Formation. Conformably overlies Samuel Formation.||
39246|Belambre Formation|24084|5|Briefly described|p146 Fig.2|Pliocene|Miocene|Misspelt - see Delambre Formation. Geological Province: North Carnarvon Basin.||||||16-MAR-05
24708|Belches Beds|23584|6|Mentioned|p37 Appendix 2|||Replaced with Mount Belches Formation. Geological Province: Yilgarn Craton.||||||
24708|Belches Beds|31040|5|Briefly described|p445|||||||||
83139|Belches Formation|72491|5|Briefly described|p4-5 Figs.3-4, p15, 19, 25-26, 31 Fig.14|||See also p44-46, 56, 60-61. Kurnalpi Terrane, Yilgarn Craton. Underwent middle-amphibolite facies metamorphism c.2656 Ma, only 10 - 15 m.y. after start of basin extension. Parageneses tabulated. Metamorphism detailed. Appears as Belches Group on p31.|||||Turbidites. Metapelite.|
77559|Belches Supersequence|66937|5|Briefly described|p155, pp160-162.|Archean|Archean|Kalgoorlie Terrane. Over 3600 m thick. Aggradational stacking implies deposition in a deep-marine linear trough with fixed-position margins.|||Includes Santa Claus Member.|Faulted against Penny Dam Supersequence.|Graded massive coarse-grained, to plane-bedded medium-grained, sandstone separated from an upper rippled fine-grained sandstone and mudrock by a horizon of banded iron formation.|
77559|Belches Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
69744|Bell Rock Gabbro|61340|5|Briefly described|Map legend|||Presented as the compound name Bell Rock Troctolite/Gabbro Intrusion.||||||
69744|Bell Rock Gabbro|70634|5|Briefly described|GA_geochron.csv|Mesoproterozoic|Paleoproterozoic|Sample description: Granophyric leucogranite.|1078 Ma +/- 3 Ma(SHRIMP), 1756 Ma (Sm-Nd)|||||
69744|Bell Rock Gabbro|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1078+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Pegmatite.|
69743|Bell Rock Troctolite|61340|5|Briefly described|Map legend|||Presented as the compound name Bell Rock Troctolite/Gabbro Intrusion.||||||
70164|Bell Rock granophyre|44109|6|Mentioned|p141 Fig. 152D|Mesoproterozoic|Mesoproterozoic|Informal reference to part of the Bell Rock intrusion. Age: 1078+/-3Ma. ||||||
75232|Bell Rock intrusion|64745|6|Mentioned|p379|||Not a formal stratigraphic unit. One of the Giles Intrusions? Found near extrusive rocks of Bentley Supergroup.||||||
75232|Bell Rock intrusion|65135|5|Briefly described|p14|Stenian|Stenian|Informal name. Broadly troctolitic. Of the Giles instrusions. Probably part of a larger single intrusion including the Blackstone and Jameson-Finlay intrusions. Granophyric leucogranite thought to be from Bell Rock intrusion dated at 1078 +/- 3 Ma by U-Pb zircon||||||
75232|Bell Rock intrusion|65693|5|Briefly described|p3.|Mesoproterozoic|Mesoproterozoic|One of a series of layered intrusions in west Musgrave Province. Includes a granophyric leucogranite, thought to be comagmatic but more likely a sill.|Minimum age 1078 +/- 3 Ma (Sun et al. 1996).|Unit in Warakurna Supersuite.||Intrudes Mummawarrawarra Basalt.|Troctolitic.|08-MAR-16
75232|Bell Rock intrusion|68996|5|Briefly described|p7, 45, 50, 52, 63, 67|Mesoproterozoic|Mesoproterozoic||1078 +/-3 Ma|Giles Suite||Connected at depth with Jameson, Cavenagh and Blackstone intrusions.|Leucogranite.|
70165|Bell Rock leucotroctolites|44109|6|Mentioned|p132|||Informal reference to the troctolites of the Bell Rock intrusion. ||||||
69752|Bell Rock troctolite/gabbro intrusion|44109|4|Described|p9, p44, p63|Mesoproterozoic|Mesoproterozoic|Informal name for part Giles Complex. Massive, troctolite, gabbroic troctolite and anorthosite; magnetite, dunite. Age: 1078+/- 3Ma (granophyre). Exposed thickness is ~3800m.||||||08-MAR-16
69752|Bell Rock troctolite/gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: ~3800m.||||||21-SEP-05
73563|Bellevue Member|63454|5|Briefly described|p71 Tb. 2|||Abbreviated version of Bellevue Limestone Member - used interchangeably in article.||||||
34415|Belvedere group|22716|6|Mentioned|p234|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
34415|Belvedere group|50226|6|Mentioned|p416|||Informal name.||||||
28058|Bent Tree basalt|23782|5|Briefly described|p8 Fig. 6|||Geological Province: Yilgarn Craton.||||||
28058|Bent Tree basalt|23926|6|Mentioned|p10 Tb. 1|||Informal.||||||
28058|Bent Tree basalt|24139|5|Briefly described|p239 Table. 1|Archean|Archean|Geological Province: Ora Banda Domain.  Of the Grants Patch Group.||||||07-NOV-08
24713|Bentley Super-Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
80375|Bentley Supergroup, lower|71210|6|Mentioned|p8-p9, p20, p22, p136||||||Includes Kunmarnara Group.|||07-FEB-18
80376|Bentley Supergroup, upper|71210|6|Mentioned|p9-p10, p20||||||Includes Tollu Group.|||07-FEB-18
34433|Bently Supergroup|22716|5|Briefly described|table4, p238|Stenian|Stenian|Age: 1080 Ma||||||
34605|Berriasian sandstone|44938|4|Described|p151, Fig.3||Berriasian|Invalid because named after age. Uncertain if name is intended to be formal or informal.||||||
37997|Bertibubba suite|23485|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Informal name.  Age: c.1960Ma.||||||07-NOV-08
37997|Bertibubba suite|23525|5|Briefly described|p4|Orosirian|Orosirian|Informal name.   Age: c.1960Ma||||||
38577|Bertibubba suite""|23781|5|Briefly described|p6|||Superseded by Bertibubba Supersuite.||||||
83188|Biberkine dyke swarm|73056|6|Mentioned|p291|Mesoproterozoic|Mesoproterozoic|Yilgarn Craton, southwest. Newly identified NNW-trending dyke swarm, designation as a dyke swarm is preliminary, see also Biberkine dykes. Aeromagnetic data suggests dyke swarm extends hundreds of kilometers in length.|1390+/-3 Ma ID-TIMS U-Pb baddeleyite||||Tholeiitic dyke swarm.|
83187|Biberkine dykes|73056|5|Briefly described|p291, 293 Fig.2, p298-299, p301|Mesoproterozoic|Mesoproterozoic|Yilgarn Craton, southwest. Newly identified NNW-trending mafic dyke swarm. Aeromagnetic data suggests dyke swarm extends hundreds of kilometers across the South West Terrane. Designation as a dyke swarm is preliminary, see also Biberkine dyke swarm p291. Preliminary geochemical analysis indicates tholeiitic composition, significant contribution from metasomatically enriched subcontinental lithosphere/lower crust. Weighted mean SHRIMP U-Pb age of 1458+/-76 Ma from 3 samples from at least two different dykes. ID-TIMS date from one sample site. Location in text includes p300 Fig.8.|1390+/-3 Ma ID-TIMS U-Pb baddeleyite||||Mafic dyke swarm, tholeiitic. Dolerite with intergranular ophitic to sub-ophitic texture comprising plagioclase, pyroxene, quartz, opaque minerals, trace apatite.|
41080|Big Blow chert|24139|5|Briefly described|p239 Table 1|||Geological Province: Boorara Domain.||||||
38580|Big Dick basalt|23782|5|Briefly described|p8 Fig. 6|||Geological Province: Yilgarn Craton.||||||
38580|Big Dick basalt|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Ora Banda Domain.  Of the Linger and Die Group.||||||07-NOV-08
77124|Biggada Sands|61554|6|Mentioned|p625 Fig.2|||Barrow Island.||||||
72412|Bililly formation|48823|6|Mentioned|p8 Fig. 1|||Informal - see Bililly Formation.||||||
83875|Billabong Basalt|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
68049|Billeringa Subgroup|24526|5|Briefly described|p114, p112 Fig. 9|Mesoproterozoic|Mesoproterozoic|Of the Moora Group.  Gently folded series of sandstone, siltstone, basalt and tuff.  Overlain by the Coomberdale Subgroup.  Age: 1500-1300Ma.  See also Billeringa Volcanics (same unit?).||||||
68049|Billeringa Subgroup|24542|5|Briefly described|p11|Mesoproterozoic|Mesoproterozoic|Of Moora Group. Sandstone, siltstone, basalt and tuff. Age: ~1390+/-140 Ma (Rb-Sr).||||||
68050|Billeringa Volcanics|24526|6|Mentioned|p114|||Probably refers to the Billeringa Subgroup? Misspelt?||||||14-JUN-05
32754|Bindoo Hill Beds|45015|6|Mentioned|p30|||May be southern extension of Tumblagooda Sandstone. Geological Province: Irwin Basin.||||||01-JUN-06
83345|Binduli Porphyry Conglomerate|73391|5|Briefly described|vii-viii, 196, 240-241, 247, 304,317-318|||See also p342, 390, 392, 395, 398, 401-402, 404-412, 414, 416, 419-420, 440-442, 444, Appendices. Ora Banda Domain. Appears as Binduli porphyry conglomerate on p175-178, 188-189, 196, 304; possibly not intended as a formal name? 90% of clasts are indistinguishable from the Centurion Porphyry. Geochemical analyses tables and plots discussed..|~2664 Ma.|Gidji Lake Formation.||Correlated with Upper Black Flag Formation/Gidji Lake formation.|Dominated by clasts of feldspar porphyry (Centurion Porphyry) with a minor component of sedimentary (mudstone and quartzite) clasts.|
24723|Binduli porphyry|30886|6|Mentioned|p29|||||||||
24723|Binduli porphyry|31038|6|Mentioned|Fig. 2|||Archaean||||||
24723|Binduli porphyry|31039|6|Mentioned|Fig. 2|||||||||
24724|Binningup calcrete|40367|6|Mentioned|p81|||Informal - see Binningup Calcrete.||||||07-AUG-07
28369|Binningup member|40367|6|Mentioned|Table 1 p72|||Informal - see Binningup Member.||||||07-AUG-07
80033|Binthalya Sandstone|67200|5|Briefly described|p7 fig 5,|Permian|Permian|||Kennedy Group||Overlies Mungadan Sandstone|Bioturbated, interbedded sandstone and siltstone with trough, planar and laminated cross beds.|
33223|Binthalya Subgroup|44537|14|Not recorded|map legend||Artinskian|||||||
33223|Binthalya Subgroup|44657|14|Not recorded|p.5,6,10|||||||||
33038|Biranup Supersuite|24197|5|Briefly described|p22, p52|Paleoproterozoic|Paleoproterozoic|Example of the Kalkadoon Association. Mostly comprised of heterogeneous orthogneisses. Age: 1700Ma. Geological province: Albany Fraser Province.||||||07-FEB-11
33038|Biranup Supersuite|50434|5|Briefly described|p1.1, 1.2, 2.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Albany-Fraser Province. Age: 1700-1600Ma.||||||07-NOV-08
38701|Birdie Creek Volcanic Member""|23867|6|Mentioned|p3|||Informal - see Birdie Creek Volcanic Member.||||||
75240|Birdrong Greensand|64973|6|Mentioned|p504|||Misspelt or obsolete name. The original use of the name was not intended to be formal.||||||16-JUN-09
74612|Birksgate Metamorphics|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1390-1330Ma. Consists of gneiss. See map legend for more information on lithology.||||||
74612|Birksgate Metamorphics|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Age <1390 Ma. Subdivided into 8 unnamed units. Geol. Province - Musgrave Complex.||||||03-MAY-13
74612|Birksgate Metamorphics|65135|6|Mentioned|p5|||Gneisses previously grouped into the Birksgate Metamorphics are included in the Wirku Metamorphics in this paper||||||
74612|Birksgate Metamorphics|65833|6|Mentioned|p5|||Rocks of Birksgate Metamorphics now grouped into Wirku Metamorphics||||||
74612|Birksgate Metamorphics|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||||Inclusions occur in Mirturtu Monzogranite.||
74612|Birksgate Metamorphics|70634|6|Mentioned|184149.1.pdf|||Reincorporated into the Wirku Metamorphics.||||||
75543|Birunup Complex|65357|6|Mentioned|p330 Fig.1|||No age information given.||||||10-DEC-09
37801|Biscay Formation basalts|24169|5|Briefly described|p670 Fig.8|Paleoproterozoic|Paleoproterozoic|Formal name not intended.||||||07-NOV-08
40042|Biscay Formation rhyolite sill""|24173|5|Briefly described|p17|||Informal name.Of the Maude Headley Member. An extrusive flow previously mapped as part of the Biscay Formation. Age: 1857 +/- 5Ma (Page & Hancock 1988).||||||06-APR-05
67828|Biscay Formation tuffs""|23383|6|Mentioned|p12|Paleoproterozoic|Paleoproterozoic|Informal - referes to tuffs of a felsic sill within the Biscay Formation.  Age: 1856+/-5Ma.||||||07-NOV-08
80319|Bitter Springs Basalt|67202|6|Mentioned|p184|||Amadeus Basin.||||||
70739|Bitter Springs Formation, lower|62453|6|Mentioned|p11|||Informal. Amadeus Basin.||||||
70724|Bitter Springs Formation, upper|62453|6|Mentioned|p11|||Informal. Amadeus Basin.||||||
70724|Bitter Springs Formation, upper|69673|6|Mentioned|p85, p89, p91|||Good potential reservoir rocks within Loves Creek Member and Johnnys Creek beds.||||||
70167|Bitter Springs Volcanics|44109|5|Briefly described|p134, p164|||Probably mispelt. Geological Province: Amadeus Basin. ||||||
70167|Bitter Springs Volcanics|62664|6|Mentioned|p137, p139. |||Amadeus Basin and Arunta Inlier.||||||
69392|Bitter Springs volcanics|61153|5|Briefly described|p344-345 Fig. 1|||Informal name. Geological Province: Amadeus Basin.||||||
83020|Black Flag Basalt|73300|6|Mentioned|p1113|||Yilgarn Craton, Kalgoorlie terrane.||||Overlies the Oroya Shale, Aberdare Dolerite, Golden Mile Dolerite, underlies [or at base of] the Black Flag Group.||
83346|Black Flag Formation, Lower|73391|5|Briefly described|p240, 194, 239, 245-247, 304, 308, 326|||See also p333, 347-350, 391, 413, 416-417, 441-443, 445, Appendices. Ora Banda Domain, Kalgoorlie Terrane. See Black Flag Formation.|~2677 Ma.||Gibson-Honman formation.|Overlies White Flag Formation or Talbot formation. Is overlain unconformably by Upper Black Flag Formation.||22-JUN-22
83347|Black Flag Formation, Upper|73391|5|Briefly described|p240-241,194, 244-247,300,304,316-318|||See also p348-350, 352, 391, 411, 413, 416-418, 441-445. Ora Banda Domain, Kalgoorlie Terrane. See Black Flag Formation.|<2663 Ma.||Gidji Lake formation.|Locally overlies Gibson-Honman formation unconformably. Is overlain unconformably by Navajo sandstone (Kurrawang Formation). Correlated with Grave Dam member, Binduli porphyry conglomerate.|Deep-water depocentres with abundant intercalated shales and turbidites.|22-JUN-22
83944|Black Flag Group, Lower|70290|6|Mentioned|p296|||Kalgoorlie district, Yilgarn Craton.|||||Carbonaceous siltstone, volcaniclastic greywacke, polymictic conglomerate.|
83932|Black Flag Group, Upper|70290|6|Mentioned|p296|||Kalgoorlie district, Yilgarn Craton.|||||Carbonaceous siltstone, volcaniclastic greywacke, polymictic conglomerate.|
82957|Black Flag Sequence|73238|6|Mentioned|p18|||Referred to as on of three lithostratigraphic packages "the Kalgoorlie Sequence (or Black Flag Sequence)".||||||28-MAR-22
82957|Black Flag Sequence|73391|6|Mentioned|p218|||||||||
34369|Black Flag Supersequence|22682|5|Briefly described|p13||Archean|Corresponds to Black Flag Group||||||07-NOV-08
33865|Black Flag beds""|22534|6|Mentioned|p9|||Previously named 'Black Flag Series', now known as Black Flag Group||||||
41034|Black Flag formation|24196|6|Mentioned|p31|||Informal - see Black Flag Formation.||||||25-MAY-04
68012|Black Flag group|23797|6|Mentioned|p5|||Informal name.||||||15-AUG-06
32625|Black Flag slates|46176|14|Not recorded|p191|||||||||
80348|Black Hill Monzogranite|70775|6|Mentioned|p49, p50|||[Mis-spelling of the Black Hill Well Monzogranite as per p15, 46, 58].||||||05-FEB-18
77787|Black Hills Yard intrusion|60498|5|Briefly described|p1016 Fig.1, p1017.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name, except for the caption referring to 'mafic-ultramafic intrusions'. Halls Creek Orogen. No mineralisation known. Small plug- and dyke-like bodies.|||||Layered mafic-ultramafic intrusion: troctolite, olivine gabbro, olivine gabbronorite, gabbro, biotite gabbro.|
77787|Black Hills Yard intrusion|69003|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Mafic intrusion that forms plug-like or dyke-like bodies.|<1830 Ma.|||||
36884|Black Range Dolerite Suite|23415|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Craton. Dolerite and medium- to coarse-grained gabbro dykes; weakly metamorphosed.||||||07-NOV-08
36884|Black Range Dolerite Suite|23757|4|Described|p13|||Age: c.2772 Ma (SHRIMP). A single, large northeasterly trending, metamorphosed medium- to coarse-grained dolerite dyke. Intrudes for a short distance the overlying Nimingarra Iron Formation.||||||20-APR-16
36884|Black Range Dolerite Suite|24531|5|Briefly described|p8-9 Fig. 3|||Of the Fortescue Group. Geological Province: Pilbara Craton.||||||22-NOV-10
36884|Black Range Dolerite Suite|50189|4|Described|p19|Archean|Archean|Of the Fortescue Group. Intrudes the Muccan and Mount Edgar Granitoid Complexes. See also Black Range Suite.||||||07-NOV-08
36884|Black Range Dolerite Suite|50544|5|Briefly described|p43-44, p15 Tb. 1|Archean|Archean|Intrudes the Muccan and Mount Edgar Granitoid Complexes.  Age: c.2772Ma (SHRIMP U-Pb baddeleyite).||||||07-NOV-08
36884|Black Range Dolerite Suite|60429|4|Described|p19|||Comprises large, north-eastery trending, medium- to coarse-grained dolerite dykes. Intruded Muccan and Mount Edgar Granitoid Complexes; smaller dykes intruded Coppin Gap Granodiorite and the overlying Warrawoona Group. Age: 2772+/-2Ma (SHRIMP U-Pb).||||||07-FEB-11
36884|Black Range Dolerite Suite|61264|5|Briefly described|p64 Fig. 2|||Geological Province: Hamersley Basin.||||||
36884|Black Range Dolerite Suite|62576|6|Mentioned|p620|Archean|Archean|See also Black Range dolerite suite. Geological province: Pilbara Craton.||||||07-NOV-08
36884|Black Range Dolerite Suite|63417|5|Briefly described|Map legend|Archean|Archean|Dolerite dyke; local gabbro; weakly metamorphosed. Geological Province: Fortescue Basin.||||||07-NOV-08
36884|Black Range Dolerite Suite|63420|5|Briefly described|Map legend|Archean|Archean|Age: c.2772Ma. Geological Province: Marble Bar Sub-basin, Hamersley Basin. Dolerite dyke, local gabbro; metamorphosed.||||||22-NOV-10
36884|Black Range Dolerite Suite|63441|5|Briefly described|p13 tb. 2, p38-39|Archean|Archean|A prominent swarm of black to very dark brown weathering dolerite dykes with north to north-east strike-related to basaltic lavas Mount Roe Basalt and Kylena Fm (of Fortescue Gp). Age: 2772+/-2Ma. Geol prov: east Pilbara Terrane/Pilbara Craton||||||07-FEB-11
36884|Black Range Dolerite Suite|63854|6|Mentioned|p229 Fig.2, p230 |Neoarchean|Neoarchean|Intrudes (stitches) the East Pilbara Terrane and Mosquito Creek Basin.|ca. 2770 Ma|||Is overlain unconformably by Fortescue Group.||
36884|Black Range Dolerite Suite|64654|5|Briefly described|Map Legend|Archaean|Archaean|Age: c. 2772Ma. Geological Province: Pilbara Craton. Dolerite dyke; local gabbro; weakly metamorphosed.||||||22-NOV-10
36884|Black Range Dolerite Suite|64656|5|Briefly described|Map Legend|Archaean|Archaean|Age: c. 2772Ma. Geological Province: Pilbara Craton. Dolerite dyke; local gabbro; weakly metamorphosed.||||||26-NOV-08
36884|Black Range Dolerite Suite|64657|5|Briefly described|Map Legend|Archaean|Archaean|Age: c. 2772Ma. Geological Province: Hamersley Basin. Dolerite dyke, local gabbro; locally metamorphosed.||||||
36884|Black Range Dolerite Suite|65008|4|Described|p8, p15, p17, p20-22|Neoarchean|Neoarchean|See also references to Black Range Dolerite suite (p7, p8 Fig.5, p41). Hamersley Basin. U-Pb zircon and baddeleyite SHRIMP age. Dykes range up to 600m in width and typically have chilled margins.|2772 +/- 2 Ma (Wingate, 1997, 1999).|Of the Fortescue Group||Unconformably underlain by the Mosquito Creek Formation?|Dolerite and medium- to coarse-grained gabbro dykes; weakly metamorphosed.|
36884|Black Range Dolerite Suite|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.|c.2772 Ma (Wingate 1999).||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|65827|3|Fully described|p12 Tb.3, p27, p30, p31-32, p40, p43|Neoarchean|Neoarchean|Intrudes Mount Edgar Granitic Complex, Corunna Downs Granitic Complex; considered part of the feeder dyke system for Mount Roe Basalt. SHRIMP U-Pb baddeleyite dates of 2772 +/ -2 Ma and 2775 +/ -5 Ma (both Wingate 1997) . NNE-trending dolerite and local gabbro dykes.||||||
36884|Black Range Dolerite Suite|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Of Fortescue Group. Fortescue Basin. c.2772 Ma. Dolerite dyke; local gabbro; weakly metamorphosed.||||||09-APR-13
36884|Black Range Dolerite Suite|66217|4|Described|p5, p6 Table 1, p46.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Sadly mis-spelled as Black Range Dolorite Suite on p5. Dykes, mainly striking NNE.|2772 +/- 2 Ma (Wingate 1999). |||Intrudes Muccan Granitic Complex.|Doleritic to gabbroic dykes.|
36884|Black Range Dolerite Suite|67130|5|Briefly described|p3 fig 2, p10, p43|Neoarchean|Neoarchean||2772 +/- 2 Ma|Fortescue Group|Includes Black Range Dyke|Intrudes Bellary Formation|Dolerite dykes.|
36884|Black Range Dolerite Suite|67201|4|Described|p28, p31|||In northern Pilbara Craton. Swarm of north-northeasterly trending dolerite dykes feeding Mount Roe Basalt.||||Swarm of dolerite dykes feeding Mount Roe Basalt.|Dolerite.|
36884|Black Range Dolerite Suite|68035|5|Briefly described|p292 Fig 6|Neoarchean|Neoarchean||2772+/-2 Ma|||Intrudes Bellary Formation, Fortescue Group and underlying unnamed basalt.|Dolerite.|
36884|Black Range Dolerite Suite|68280|5|Briefly described|p5, p36, p40|Neoarchean|Neoarchean||2772+/- 2 Ma|Fortescue Group||Overlain by Mount Roe Basalt|Dolerite dykes and sills.|13-JAN-23
36884|Black Range Dolerite Suite|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean||c. 2772 Ma (Wingate 1999).||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c. 2772 Ma (Wingate, 1999).||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.|c. 2772 Ma (Wingate, 1999).|Of the Fortescue Group|||Dolerite dyke; local gabbro; metamorphosed.|16-JUN-14
36884|Black Range Dolerite Suite|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c. 2772 Ma (Wingate, 1999)||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|69013|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c. 2772 Ma (Wingate 1999)||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c. 2772 Ma (Wingate, 1999)||||Dolerite dyke; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|69041|4|Described|p11, p18|Archaean|Archaean|Pilbara Craton. Of the Corunna Downs Igneous Complex and the Mount Edgar Igneous Complex (which are used in the province sense:. Forms prominent ridges trending north-northeast. Dykes vary in width from 50m up to 200m. Contact metamorphism occurs within 3m and the metamorphic aureole can extend up to 70m.|2772 +/- 2 Ma (SHRIMP, Wingate, 1999)||||Medium- to coarse-grained, dolerite and gabbro dykes with marked chilled margins and contact metamorphosed with the country rock.|21-JUN-19
36884|Black Range Dolerite Suite|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean||||||Dolerite dyke; local gabbro; weakly metamorphosed|
36884|Black Range Dolerite Suite|69301|4|Described|p16|||In northern Pilbara Craton. |2.78 Ga|||Field relations and geochronology indicate that these dykes fed extrusion of the Mount Roe Basalt.|Suite of dolerite dykes.|
36884|Black Range Dolerite Suite|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: West Australian Craton. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|2772 Ma (isotopic)||||Dolerite dyke; local gabbro; weakly metamorphosed|
36884|Black Range Dolerite Suite|70795|5|Briefly described|2_5m_interpdykel15_lut.csv|Neoarchean|Neoarchean||2772 Ma||||Dolerite; local gabbro; weakly metamorphosed.|
36884|Black Range Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Neoarchean|Neoarchean|East Pilbara Craton.|2772 Ma|||||
36884|Black Range Dolerite Suite|70884|5|Briefly described|p132|Neoarchean|Neoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Also referred to in text as Black Range Sdyke Swarm. Associated with Fortescue Group. Includes a mafic mega dyke intuded into the Doolena Gap Greenstone Belt, with dextral strike separation of c. 1.2km.|~2.78 Ga|||||
36884|Black Range Dolerite Suite|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||dolerite, gabbro|
36884|Black Range Dolerite Suite|71808|5|Briefly described|p7, p47|||Synvolcanic with the Mount Roe Basalt.|2772 +/- 2 Ma (Wingate, 1997)|||||
36884|Black Range Dolerite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Marble Bar Sub-basin; Northeast Pilbara Sub-basin; Northwest Pilbara Sub-basin; South Pilbara Sub-basin, Fortescue Basin.|2772+/-2 Ma.||||Dolerite dyke; local gabbro; weakly metamorphosed.|
39602|Black Range Dolerite suite|24532|5|Briefly described|Map legend|Archean|Archean|Age: c.2772Ma.||||||07-NOV-08
39602|Black Range Dolerite suite|50381|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2772 Ma||||||07-NOV-08
39602|Black Range Dolerite suite|50555|5|Briefly described|Map legend|Archean|Archean|Dolerite and medium to coarse-grained gabbro dykes; weakly metamoprhosed.  Age: c.2772Ma.   Geol. Province: Hamersley Basin.||||||07-NOV-08
39602|Black Range Dolerite suite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Age: 2772Ma. Geological Province: Pilbara Craton. Dolerite and medium- to coarse-grained gabbro dykes; weakly metamorphosed.||||||07-FEB-11
39602|Black Range Dolerite suite|64936|5|Briefly described|map legend|Archean|Archean|Informal name. ?Of Fortescue Group. Intrudes Pilbara Supergroup. Age: c. 2772 Ma (geochronology: MTD Wingate 1999). Geol. Prov: Hamersley Basin, Pilbara Craton.||||||17-DEC-12
39602|Black Range Dolerite suite|65008|4|Described|p7, p8, p15 Tb.1, p17, p20-22, p41|Neoarchean|Neoarchean|See also references to Black Range Dolerite Suite (p8, p15, p17, p20-22). Hamersley Basin. U-Pb zircon and baddeleyite SHRIMP age. Dykes range up to 600m in width and typically have chilled margins.|2772 +/- 2 Ma (Wingate, 1997, 1999).|Of the Fortescue Group||Unconformably underlain by the Mosquito Creek Formation?|Dolerite and medium- to coarse-grained gabbro dykes; weakly metamorphosed.|14-MAY-14
39602|Black Range Dolerite suite|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.|c.2772 Ma (Arndt et al. 1991).|Of Fortescue Group.|||Dolerite and medium- to coarse-grained gabbro dykes; weakly metamorphosed.|
37146|Black Range Doleritic Suite|23755|5|Briefly described|p56, p58|Archean|Archean|Age: c.2772 Ma.||||||07-NOV-08
36954|Black Range Dolomite Suite|23585|5|Briefly described|p10 Table 1|||||||||
32779|Black Range Dolomite suite|44229|5|Briefly described|Map Legend|Archean|Archean|Part of the Fortescue Group.  Dolerite and medium- to coarse-grained gabbro dykes.||||||07-NOV-08
32453|Black Range Dyke|31308|5|Briefly described|p.68-73.|||Part of the Pilbara Region. Table 12 geochronology.||||||
32453|Black Range Dyke|67130|6|Mentioned|p43, p45|||||Black Range Dolerite Suite||||
73874|Black Range Dyke Suite|24590|5|Briefly described|p50, p91 Fig. 3.7|Archean|Archean|Basaltic intrusive rocks. Age: 2772+/-2Ma and ca.2.80-2.75Ga. See also Black Range Suite. Names used interchangeably. Also referred to as the Black Range Dyke Swarm (p51).||||||01-AUG-12
73874|Black Range Dyke Suite|62129|6|Mentioned|p4, p22|||||||||07-FEB-11
73874|Black Range Dyke Suite|64384|6|Mentioned|p25, p26|||Located in northern Pilbara and described by Hickman (1975). Informal name; also referred to as Black Range suite.||||||07-FEB-11
80619|Black Range Dyke Swarm|71803|6|Mentioned|p368||||2772 +/- 2 Ma|||||
34039|Black Range Dykes|22475|4|Described|p493-498|Archean|Archean|See also Figure 1-5, Table.1||||||07-NOV-08
34039|Black Range Dykes|73598|6|Mentioned|p1208-1209|||East Pilbara Terrane. Includes reference to Black Range dyke swarm.||||||
29951|Black Range Suite|23570|5|Briefly described|p24|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
29951|Black Range Suite|23783|5|Briefly described|p110|Archean|Archean|Age: c.2772Ma.||||||07-NOV-08
29951|Black Range Suite|24025|6|Mentioned|p14|||Geological Province: Hamersley Basin.||||||
29951|Black Range Suite|24590|5|Briefly described|p69|Archean|Archean|Dolerite dykes. Age: 2772+/-2Ma. See also Black Range Dyke Suite. Names used interchangeably.||||||07-FEB-11
29951|Black Range Suite|43055|6|Mentioned|p12|||||||||
29951|Black Range Suite|43644|6|Mentioned|p592|||||||||
29951|Black Range Suite|50131|6|Mentioned|p2, p4 Fig. 2, p8, p9, p12, p15|||Age: 2772+/-2Ma (SHRIMP).||||||22-APR-09
29951|Black Range Suite|50189|6|Mentioned|p19|||Abbreviation of Black Range Dolerite Suite? Age: 2772 +/- 2Ma (Wingate, 1997).||||||
29951|Black Range Suite|60373|5|Briefly described|p152, p165 Fig. 7|Archean|Archean|Age: 2772+/-2 Ma (Pb/Pb, Wingate, 1991).||||||
29951|Black Range Suite|60429|6|Mentioned|p19|||Informal - see Black Range Dolerite Suite.||||||07-FEB-11
34331|Black Range Suite""|22717|6|Mentioned|P11||Siderian|Age of unit is 2329+/-89 Ma||||||
40504|Black Range dolerite suite|24531|6|Mentioned|p36|||Informal - see Black Range Dolerite Suite.||||||
40504|Black Range dolerite suite|62576|5|Briefly described|p618 Fig. 1, p619|Archean|Archean|Informal - see Black Range Dolerite Suite. Geol.prov: Pilbara Craton. This is a 'feeder' for volcanic rocks of lower part of Fortescue Group. The Black Range dolerite dyke is 300m wide and has been dated at 2772Ma; extends across Shaw Granitoid Complex. ||||||07-NOV-08
38748|Black Range suite|24025|6|Mentioned|p15|||Informal - see Black Range Suite.  Geological Province: Hamersley Basin.||||||
38748|Black Range suite|64724|5|Briefly described|p42|Neoarchean|Neoarchean|Dolerite dykes intruded during extension of the Hamersley Basin. Dated at ~2772 Ma (Wingate 1999)||||||
78962|Black Rock Tonalite|44155|5|Briefly described|p239 Tb.3-3, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|East Kimberley.||Lamboo Complex|||Coarse-grained porphyritic biotite-hornblende tonalite.|15-JAN-15
69765|Blackstone Range troctolite/gabbro intrusion|44109|4|Described|p10, p85|Mesoproterozoic|Mesoproterozoic|Informal part Giles Complex. Highly fractionated, rhythmically layered troctolite, olivine gabbro, anorthosite, rare dunite layers and monomineralic magnetite layers. Max. thickness: >3600m.||||||
69765|Blackstone Range troctolite/gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: ~3600m.||||||
69738|Blackstone Troctolite|61341|5|Briefly described|Map legend|||Presented in the compound name Blackstone Range Troctolite/Gabbro. Intrusion.||||||21-SEP-05
77410|Blackstone intrusion|65135|5|Briefly described|p14, p16|||Informal name. Broadly troctolitic. Of the Giles intrusions. Probably part of a larger single intrusion including the Bell Rock and Jameson-Finlay intrusions. Includes xenoliths of Mummawarrawarra Basalt. Overlain by Smoke Hills Volcanics||||||15-MAY-14
77410|Blackstone intrusion|65693|5|Briefly described|pp3-4. |Mesoproterozoic|Mesoproterozoic|One of a series of layered intrusions in west Musgrave Province. Forms most of Blackstone Range.|>1078 Ma.|Unit in Warakurna Supersuite.||Intrudes Mummawarrawarra Basalt.|Troctolitic.|
77410|Blackstone intrusion|67128|5|Briefly described|p20, p23, p25, p31|||||||Is overlain by Tollu Group.|Layered mafic-ultramafic intrusion.|
77410|Blackstone intrusion|68996|5|Briefly described|p39, 41-43,45,50,52,56,57,62,63,64,65,67|Mesoproterozoic|Mesoproterozoic|See also Blackstone-Cavenagh intrusion p47.||Giles Suite?||Connected at depth with Jameson, Cavenagh and Bell Rock intrusions.||
32968|Blackwood Shale|44303|14|Not recorded|p.9||Mesozoic|(I/50-5,9).||||||
78535|Blatchford Formation""|13194|6|Mentioned|p395 tab 4-16|||Of Ord Basin? or Bonaparte Basin?. Part included in Cambrian Tarrara Formation.||||||27-NOV-13
29413|Bloods Range beds|22561|4|Described|p15|Neoproterozoic|Neoproterozoic|||||||
29413|Bloods Range beds|22567|6|Mentioned|p91|||||||||
29413|Bloods Range beds|22804|6|Mentioned|Fig 2 on p432|||||||||
29413|Bloods Range beds|23716|6|Mentioned|p4|||||||||
29413|Bloods Range beds|24301|6|Mentioned|p14|||Scrimgeour et al, 2000.||||||
29413|Bloods Range beds|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, slate, tuff, basalt, felsic porphyry and metamorphic equivalents.  Geological province: Amadeus Basin.||||||07-NOV-08
29413|Bloods Range beds|43503|6|Mentioned|12||Proterozoic|||||||
29413|Bloods Range beds|44139|5|Briefly described|p284, 285 Fig. 3-69|||Deformed and metamophosed sandstone, siltstone, shale, tuff, basalt, porphyry. Overlies  Mount Harris Volcanics. Correlated with Dixon Range beds.| | ||||10-SEP-12
29413|Bloods Range beds|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Gritty to pebbly quartz-muscovite schist, schistose quartz conglomerate, muscovite-phlogopite-epidote-quartz+/-kyanite schist, rare phyllite and quartzite.||||||08-FEB-05
29413|Bloods Range beds|60683|4|Described|p23-24, p9 Tb. 1|Mesoproterozoic|Mesoproterozoic|See also Bloods Range Beds. Gritty quartz-muscovite schist, schistose quartz conglomerate, kyanite-muscovite-epidote-quartz schist, rare phyllite and quartzite. Overlain by Dean Quartzite; overlie Wankari volcanics. Geological Province: Musgrave Block.||||||20-APR-05
29413|Bloods Range beds|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
29413|Bloods Range beds|62359|6|Mentioned|p549, p550|||See also Bloods Range Beds. Overlie Dean Quartzite or Pinyinna Beds. Geological Province: Amadeus Basin. ||||||
29413|Bloods Range beds|63562|6|Mentioned|p341|||Of Amadeus Basin. Part of the initial Basin fill.||Tjauwata Group.||||
29413|Bloods Range beds|65102|6|Mentioned|p363, Figure 4-38|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.||||||
29413|Bloods Range beds|65256|6|Mentioned|p6 Tb.1, p13|||Equivalent to the lower section of Tjauwata Group; now known as Bloods Range Formation.||||||
29413|Bloods Range beds|67856|6|Mentioned|p339 fig 4-31|||Shown as roughly equivalent to Dixon Range beds.||||||
29413|Bloods Range beds|69436|6|Mentioned|p21:13|||Forman (1966). Now Bloods Range Formation.||||||12-JUL-16
70757|Bloods Range beds''|62453|6|Mentioned|p54|||Informal name.||||||
28379|Blue Bird Gabbro sill|30900|6|Mentioned|p70|||||||||
83348|Bluebush Sequence|73391|6|Mentioned|Appendices.|||Gresham and Loftus-Hills (1971). Regional stratigraphic correlation chart of other workers.|||||Footwall basalt, ultramafic rocks, hangingwall basalt.|
42070|Bluehole Formation|23809|5|Briefly described|p47|Proterozoic|Proterozoic|See also Blue Hole Fm. Tuffite. Conformably overlain by Campbell Springs Dolostone; conformably overlies Farquharson Sst.  Age: 1636+/-5Ma.  Max. thick: ~133m. Geol.Prov: Victoria-Birrindudu Basins.||||||10-NOV-04
42070|Bluehole Formation|64737|5|Briefly described|p243|Statherian|Statherian| U-Pb date on a volcaniclastic unit.|1636 +/- 5 Ma (Smith, 2001).|Of Limbunya Group.||||01-MAY-12
42071|Bluehole Formation tuff|23809|6|Mentioned|p49|||Informal - see Bluehole Formation.||||||
27344|Bocrabee Sandstone|23594|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Renamed Googhenama Formation.||||||
27344|Bocrabee Sandstone|23746|5|Briefly described|p8 Fig 5|Proterozoic|Proterozoic|Renamed Googhenama Formation.||||||01-DEC-11
27344|Bocrabee Sandstone|30881|5|Briefly described|p527|||||||||
27344|Bocrabee Sandstone|33849|6|Mentioned|p124|||||||||
27344|Bocrabee Sandstone|34135|4|Described|Table 2|||Middle Proterozoic||||||
27344|Bocrabee Sandstone|36881|4|Described|p117|||See also P118.||||||
27344|Bocrabee Sandstone|37212|6|Mentioned|p10|||||||||
27344|Bocrabee Sandstone|37460|6|Mentioned|p173|||||||||
27344|Bocrabee Sandstone|37707|6|Mentioned|p14|||See also Table I.||||||
27344|Bocrabee Sandstone|39424|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27344|Bocrabee Sandstone|39426|4|Described|p13|||||||||
27344|Bocrabee Sandstone|41669|6|Mentioned|p46|||||||||
27344|Bocrabee Sandstone|42352|5|Briefly described|p29, p15|||Old name replaced by Googhenama Formation||||||
27344|Bocrabee Sandstone|44139|6|Mentioned|p277, p279|||de la Hunty (1963), abandoned. Rocks now included in Googhenama Formation (Chin et al. 1980; Williams 1989).| | ||||05-MAR-18
27344|Bocrabee Sandstone|44297|14|Not recorded|p.5,7,12,18,19|||(F51-9).||||||
27344|Bocrabee Sandstone|44298|14|Not recorded|map legend||Proterozoic|||||||
27344|Bocrabee Sandstone|46319|5|Briefly described|p16|||Superseded by Coolbro Sandstone.||||||
29654|Bogadi Sandstone|43015|6|Mentioned|p317|||Variation on Bogadi Greywacke?||||||
39723|Bokingarra Group|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Misspelt - see Bookingarra Group. Geological Province: Mallina basin||||||07-NOV-08
39723|Bokingarra Group|24190|6|Mentioned|p820 Fig.1|||||||||
23403|Boll Creek Conglomerate|40993|6|Mentioned|Fig.1|||||||||
82944|Bonaparte Group|73255|6|Mentioned|p533 Fig.1|Devonian|Devonian|||||||
39655|Bongabinni formation|24449|5|Briefly described|p739|||Informal - see Bongabinni Formation.  Of Carribuddy Group.  Geological Province: Canning Basin.||||||
39714|Bongabinni formation, lower|24449|6|Mentioned|p749, 750|||Informal - see Bongabinni Formation.||||||
39715|Bongabinni formation, upper|24449|6|Mentioned|p746|||Informal - see Bongabinni Formation.||||||
23406|Bonney Downs Granite|24193|5|Briefly described|p878 Tb.1|Archean|Archean|Parent: Kurrana granitoid complex. Geological Province: Pilbara Craton||||||07-NOV-08
23406|Bonney Downs Granite|37633|6|Mentioned|Plate 1|||||||||
23406|Bonney Downs Granite|39697|3|Fully described|p47|||See also Fig.31||||||
23406|Bonney Downs Granite|44150|5|Briefly described|p146 Tb.2-21|||375 sq. km. Sn, Ta, Be in pegmatite.||Kurrana Granitoid Complex|||Syenogranite.|
23406|Bonney Downs Granite|50287|5|Briefly described|Map Legend|Archean|Archean|Of Kurrana Granitoid Complex. Geological Province: Kurrana Terrane, Pilbara Craton. Monzogranite, medium grained, sparsely porphyritic; locally muscovite bearing.||||||07-NOV-08
23406|Bonney Downs Granite|61264|6|Mentioned|p65 Tb. 1|||||||||
23406|Bonney Downs Granite|63417|5|Briefly described|Map legend|Archean|Archean|Of Split Rock Supersuite. Geological Province: Pilbara Craton. Monzogranite, medium-grained, sparsely porphyritic; locally muscovite-bearing.||||||07-NOV-08
23406|Bonney Downs Granite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Superseded by Bonney Downs Monzogranite (Split Rock Supersuite). Geological province: Pilbara Craton.||||||07-FEB-11
23406|Bonney Downs Granite|63854|6|Mentioned|p230, p233 Tb.1.|Mesoarchean|Mesoarchean|Kurrana Terrane. Post-tectonic.|ca. 2838 Ma|Of the Split Rock Supersuite.||||
23406|Bonney Downs Granite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Kurrana Granitoid Complex. Age: c. 2838Ma. Geological Province: Pilbara Craton. Monzogranite, medium grained, sparsely porphyritic, locally muscovite-bearing.||||||07-FEB-11
23406|Bonney Downs Granite|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Split Rock Supersuite. Age: c. 2838Ma. Geological Province: Pilbara Craton. Medium-grained monzogranite; sparsley porphyritic; locally muscovite-bearing.||||||26-NOV-08
23406|Bonney Downs Granite|65008|4|Described|p7, p16, p21, p24, p41|Mesoarchean|Mesoarchean|Kurrana Terrane. Geochronology by: D.R. Nelson, in prep, GSWA Record. Age from a sample of biotite monzogranite. Also older Sm-Nd dates (3280, 3260 Ma) [but said to intrude Golden Eagle Orthogneiss which is ~3199-3178 Ma].|2838 +/- 6 Ma (U-Pb zircon SHRIMP).|Of the Split Rock Supersuite||Intrudes the Golden Eagle Orthogneiss.|Weakly foliated, fine- to medium-grained, sparsely porphyritic biotite monzogranite, with locally abundant xenoliths of granitic gneiss.|06-APR-16
23406|Bonney Downs Granite|65825|5|Briefly described|p6, p7 Fig.4, p12, p18, p31.|Archean|Archean|One of a group of late- to post-tectonic Sn-Ta-Li-bearing monzogranites ('tin granites') emplaced across East Pilbara Granite-Greenstone Terrane and Kurrana Terrane at 2.89 - 2.83 Ga. Appendix 2 presents this as a unit in the Split Rock Supersuite according to the GSWA databases. Affected by dextral shearing during deformation between c.2860 - 2775 Ma. |c.2860 Ma.|Unit in Kurrana Granitic Complex.||||
23406|Bonney Downs Granite|65828|5|Briefly described|Map legend|Archean|Archean||c.2838 Ma.|Unit in Kurrana Granitoid Complex.|||Medium-grained, sparsely porphyritic monzogranite; locally muscovite-bearing; strongly foliated along Coondamar Fault.|
83855|Bonnievale Granite|65834|6|Mentioned|p49-50|||Coolgardie Goldfield. Also mis-spelt as Bonnievale Group on p50.||||||
83349|Bonnivale Tonalite|73391|5|Briefly described|p302|||North Kalgoorlie district. [A mis-spelling of Bonnievale Tonalite.] The oldest felsic intrusive rock in the study area.|2680 +/- 5 Ma (SHRIMP: Hill et al., 1992).||||A 1.5 x 1.5 km stock.|
80888|Booaloo Granodiorite|71869|5|Briefly described|p7|||Capricorn Orogen.|1785 Ma (igneous crystalisation age)|Moorarie Supersuite|||Biotite granodiorite.|
73875|Boodalana Suite|24590|6|Mentioned|p71 Fig. 2.18|||Misspelt - see Boodallana Suite.||||||07-FEB-11
78505|Boodanoo Mafic-Ultramafic Suite|68110|6|Mentioned|p673, p674 Fig.2|||Variation on Boodanoo Suite (p686).||||||
69627|Boogardie orbicular granite|61273|6|Mentioned|p87|||Not a formal stratigraphic name. An ornamental stone.||||||17-MAY-06
81217|Bookargemoona Suite|69041|4|Described|p10, p19, 21, 22|Archean|Archean|Pilbara Craton. Of the Corunna Downs Igneous Complex (used in the province sense). Forms an elliptical shaped body in the northwest of the Complex. Outcrop varies from scattered boulders to slabs and is locally well exposed in rivers. This suite contains six unnamed members. Monzogranite and granodiorite have moderate radiometric total counts and low magnetic susceptibilities.|||||Fine to coarse-grained, hornblende-biotite monzogranite to biotite-hornblende granodiorite with a seriate to sparsely developed porphyritic feldspar texture. Minor xenoliths and veins occur.|21-JUN-19
70133|Bookingarra Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (Pilbara Supergroup). Contains the Salt Well Member. Geological Province: Pilbara Craton.||||||07-NOV-08
70133|Bookingarra Formation|63441|2|Defined|p46 Appx.1, p5 Tb.1, p27|Archean|Archean|Of Croydon Gp (Pilbara Supergp). Formerly Bookingarra Group. Includes Louden + Mount Negri Volcanic Members. Overlies Cistern Fm. Age:c.2955Ma (younger than c.2964Ma, older than c.2948Ma).Geol.prov: Mallina Basin/Pilbara Craton. Siliceous high-Mg basalt.||||||07-FEB-11
70133|Bookingarra Formation|63538|4|Described|p10, p16, p32, p35, p6 Fig. 3, p9 Fig. 3|Archean|Archean|Of Croydon Group (De Grey Supergroup). Overlain by Cattle Well Formation. Geological Province: Pilbara Craton. Mafic volcanic rocks.||||||19-APR-13
70133|Bookingarra Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup). Includes Louden Volcanic Member, Comstock Member and Mount Negri Volcanic Member. Geological province: Mallina Basin.||||||07-NOV-08
70133|Bookingarra Formation|64580|6|Mentioned|map legend||Mesoarchean|||||||
70133|Bookingarra Formation|64632|6|Mentioned|p203|Mesoarchean|Mesoarchean|Mallina Basin||Of the Croydon Group |Includes Louden Volcanic Member, Mount Negri Volcanic Member|basalts are extrusive equivalent of the Langenbeck Suite.||
70133|Bookingarra Formation|66217|5|Briefly described|pp38-39, p42, p43.|||Mallina Basin. Described also as 'silicic, high-Mg basalts'.||Unit in Croydon Group.|Includes Coonieena Basalt Member.||Mafic volcanics.|
70133|Bookingarra Formation|67201|4|Described|p7, p12, p16-17, p21 Fig.12 see comments|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin. Two volcanic members (lower Mount Negri Volcanic Member and upper Louden Volcanic Member) show slight, but persistent, geochemical differences and are easily distinguished in the field. Misspelt as Bookingarra Group on p63. Page location continued: p23, p57, p59-61, p63.|Min age: 2943+/-7 Ma of overlying Kialrah Rhyolite|Croydon Group|Mount Negri Volcanic Member, Louden Volcanic Member, South Mallina Basalt Member, Salt Well Member, Yareweeree Member, Coonieena Basalt Member|Louden Volcanic and Mount Negri Volcanic Members (Bookingarra Formation) overlie (and overlap with) Rushall Slate in Whim Creek greenstone belt.|Commonly pillowed mafic lava flows (siliceous high-Mg basalt), with thin laminated mudstone and sandstone intervals locally interlayered, and contacts are peperitic.|
70133|Bookingarra Formation|68035|5|Briefly described|p291|Mesoarchean|Mesoarchean|Mallina Basin.||Of Croydon Group.|||Volcaniclastic and mafic-felsic volcanic rocks.|
70133|Bookingarra Formation|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins.|3020-2948 Ma|Of the Croydon Group.|Includes Salt Well Member.||Mafic volcanic and intrusive rocks; includes debris-flow deposits; metamorphosed.|
70133|Bookingarra Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of Croydon Group.|Includes Comstock Member, Louden Volcanic Member, Mount Negri Volcanic Member.|||
70133|Bookingarra Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p15|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Mallina Basin.||Croydon Group||Overlies Rushall Slate.|Mafic volcanic rocks. Composed of two siliceous high-Mg basalt members.|
70133|Bookingarra Formation|69590|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton. Of De Grey Superbasin. Events: North Pilbara Orogeny. See 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.||Unit of Croydon Group.|Includes Louden Volcanic Member.|||
70133|Bookingarra Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
70133|Bookingarra Formation|70775|6|Mentioned|p45, p56, p94|||According to the authors this is an obsolete term derived from Van Kranendonk et al., 2006 and should be replaced by the Louden and Mount Negri Volcanics of the reinstated Bookingarra Group.||||||
70133|Bookingarra Formation|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Mount Negri Volcanic Member, Louden Volcanic Member, South Mallina Basalt Member.|||
70133|Bookingarra Formation|72668|5|Briefly described|p4, p8, p14-15, p21-22|||West Pilbara Superterrane, East Pilbara Terrane.||Croydon Group.|Includes the Coonieena Basalt Member and the Louden and Mount Negri volcanic members.|Overlain by the Cattle Well Formation and the Kialrah Rhyolite. Overliues the Rushall Slate.||12-JAN-22
33918|Bookingarra Granite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2925 Ma||||||07-NOV-08
33918|Bookingarra Granite|23784|5|Briefly described|p20|Archean|Archean|Of Caines Well Granitoid Complex.  Age: c.2925+/-4Ma.||||||07-NOV-08
33918|Bookingarra Granite|23793|6|Mentioned|p32|||||||||
33918|Bookingarra Granite|23794|5|Briefly described|Map Legend|Archean|Archean|Of Caines Well Granitoid Complex. Geological Province Pilbara Craton.||||||07-NOV-08
33918|Bookingarra Granite|23813|6|Mentioned|p90 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33918|Bookingarra Granite|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.2.925 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
33918|Bookingarra Granite|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33918|Bookingarra Granite|24140|6|Mentioned|p215, p223 Fig. 5|||||||||
69725|Bookingarra group|24140|6|Mentioned|p217 Fig. 2, p229|||Informal - see Bookingarra Granite.||||||
33922|Boolaloo Granitoid|22484|6|Mentioned|p74|||||||||
31953|Boolaloo Supersuite|24197|5|Briefly described|p69, p71 Tb. 7.1|Paleoproterozoic|Paleoproterozoic|Parts of this supersuite may be incorporated into the Minnie Creek Supersuite. Includes the Boolaloo, Jundelaya Hill and Mount Danvers Granodiorites and the Kilba and Hooley Granites. Age: 1800Ma.||||||07-FEB-11
31953|Boolaloo Supersuite|50425|5|Briefly described|p1.1, 1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province.  Age: 1800Ma.||||||07-NOV-08
79178|Boolgadeena Iron Member|65757|6|Mentioned|p88|||[Misspelling of Boolgeeda Iron Formation] Age: 2445+/-5 Ma.||||||
29779|Boolgeeda Iron-formation|43037|6|Mentioned|Table 1 p24|||Misspelling of Boolgeeda Iron Formation||||||
29779|Boolgeeda Iron-formation|64725|6|Mentioned|p58.|||||Topmost unit in Hamersley Group.||Overlies Woongarra Rhyolite.||
83178|Boonadgin dykes|73056|6|Mentioned|p291, p293 Fig.2, p297-299, p300 Fig.8|Orosirian|Orosirian|Yilgarn Craton, southwest. See also Boonadgin dyke swarm p301.|1888 Ma|||||
83178|Boonadgin dykes|73057|6|Mentioned|p1-2|Orosirian|Orosirian|Yilgarn Craton.|1888 Ma||||Mafic dykes.|
36980|Boonadwari Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Savory Group. Geological Province: Savory Basin.||||||
35235|Boondawari Dolerite""|23156|6|Mentioned|p18|||Rb-Sr isotopic date of ~640 Ma.||||||
35235|Boondawari Dolerite""|50188|6|Mentioned|p17|||Of Williams (1992).  Intruded Boondawari Formation.||||||16-JUL-08
70758|Boondawari Dolerite''|62453|6|Mentioned|p70|||Also called Boondawari dolerite''. ||||||
76112|Boondawari dolerite""|65337|6|Mentioned|p94.|||Also called Boondawari Dolerite||Unit in Kalkarindji Volcanic Group.||||
39288|Boondawarri Formation|24161|5|Briefly described|p14|||Max. Thickness: ~800m. Geological Province: Officer Basin. Stratigraphic equivalent of the Wahlgu Formation.||||||
39288|Boondawarri Formation|24246|5|Briefly described|p17|Proterozoic|Proterozoic|Overlies Mundajini Formation, overlain by McFadden Formation. Geological Province: Savory Basin.||||||
39288|Boondawarri Formation|50228|5|Briefly described|p489|Neoproterozoic|Neoproterozoic|Age: c.610Ma. Geological Province: Officer Basin.||||||
39288|Boondawarri Formation|64283|5|Briefly described|p49, p51 Fig. 2|||Overlies the Sunbeam Group. Geological Province: Officer Basin.||||||07-FEB-11
39288|Boondawarri Formation|64286|5|Briefly described|p73 Fig. 2|||Geological province: Officer Basin.||||||07-FEB-11
39288|Boondawarri Formation|64589|6|Mentioned|dated_samples file||Cambrian|Dolerite intruding the diamictite of this formation dated by SHRIMP on zircon. Crystallization age of dolerite 508+/-5 Ma.||||||
39288|Boondawarri Formation|64793|6|Mentioned|p283 fig 2|Neoproterozoic|Neoproterozoic|Of NW Officer Basin.|||||Diamictite, cap dolomite, sandstone, siltstone, dolomite.|
39288|Boondawarri Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
27719|Boongerooda Greensand|23311|5|Briefly described|map legend|Paleocene|Paleocene|of Cardabia Group.||||||
27719|Boongerooda Greensand|23815|4|Described|p299, 300|Paleocene|Paleocene|Geological Province: Carnarvon Basin. Basal unit of the Cardabia Group. Underlain by Miria Marl (disconformable). Overlain by Wadera Calcarenite (conformable). Max. thickness: 3 m.||||||05-MAY-08
27719|Boongerooda Greensand|24059|5|Briefly described|p138|Tertiary|Tertiary|Geological Province: Exmouth Sub-basin.||||||
27719|Boongerooda Greensand|24094|4|Described|p268, p275|Late Paleocene|Late Paleocene|Name used interchangably with Boongerooda Greensand Member. Of the Cardabia Formation. Overlies disconformably the Miria Formation. Geological Province: Carnarvon Basin||||||16-MAR-05
27719|Boongerooda Greensand|31396|6|Mentioned|p1183|||||||||
27719|Boongerooda Greensand|32648|6|Mentioned|p32|||Cardabia Gp.||||||
27719|Boongerooda Greensand|34343|5|Briefly described|p94|||Middle Paleocene||||||
27719|Boongerooda Greensand|35105|6|Mentioned|Fig.64|||||||||
27719|Boongerooda Greensand|35282|6|Mentioned|p27|||||||||
27719|Boongerooda Greensand|36257|6|Mentioned|Table 2.1|||||||||
27719|Boongerooda Greensand|36890|3|Fully described|p300|||||||||
27719|Boongerooda Greensand|37016|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
27719|Boongerooda Greensand|38444|6|Mentioned|p300|||||||||
27719|Boongerooda Greensand|39427|4|Described|Table 1|||||||||
27719|Boongerooda Greensand|40144|6|Mentioned|p306|||||||||
27719|Boongerooda Greensand|40617|6|Mentioned|p14|||||||||
27719|Boongerooda Greensand|42123|5|Briefly described|p37|||||||||
27719|Boongerooda Greensand|42473|6|Mentioned|p9|||||||||
27719|Boongerooda Greensand|42563|5|Briefly described|Fig.26 P165|||||||||
27719|Boongerooda Greensand|42995|5|Briefly described|p37|||||||||
27719|Boongerooda Greensand|44232|14|Not recorded|p13,16|||||||||
27719|Boongerooda Greensand|44657|14|Not recorded|p.5,6,12,13|||||||||
27719|Boongerooda Greensand|44996|14|Not recorded|p.10,12||Tertiary|Disconformably overlies Miria Marl, post-Cretaceous, Cretaceous - Tertiary boundary at base.||||||
27719|Boongerooda Greensand|45015|5|Briefly described|map legend|Tertiary|Tertiary|Of the Cape Range Group. Age is Late Tertiary.||||||01-JUN-06
27719|Boongerooda Greensand|48831|14|Not recorded|p.81|||||||||
27719|Boongerooda Greensand|61958|5|Briefly described|Map sheet 1|Paleogene|Paleogene|||||||
80833|Boord Formation""|71088|6|Mentioned|p8, p15|Neoproterozoic|Neoproterozoic|Amadeus Basin. This unit was originally correlated with the Carnegie Formation. Subsequently correlated with older succession (see p8). Name now disused. Shown as replaced by all of Wallara Formation, Areyonga Formation, Aralka Formation, Olympic Formation, Pertatataka Formation, Julie Formation succession, p8.||||||07-MAR-19
70216|Boorthanna chert|61579|5|Briefly described|p77|Neoproterozoic|Neoproterozoic|Informal name. Contains degraded remains of Eoentophysalis colonies. Age:ca 900Ma. ||||||
77481|Borde Marl Member|60385|5|Briefly described|p270, p272 Fig 3|Campanian|Campanian|Browse Basin. Slope and basinal deposits. See also Borde Marl p276.|p281|Turnstone Formation||Shown as having seperate instances of Puffin Sandstone Member both underlying and overlying.||01-SEP-14
70458|Borde formation|60709|5|Briefly described|p829|Maastrichtian|Campanian|Informal name. Siliciclastic rocks - of interbedded calcareous claystones and submarine fan sandstones. Geological province: Vulcan Sub-basin.||||||
72659|Borde/Prudhoe Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Informal compound term to include both Puffin Formation and Prudhoe Formation.  Age: ~71-~63Ma. Geological Province: Londonderry High.||||||09-NOV-06
38651|Bore Well complex|23786|5|Briefly described|p20|Archean|Archean|Informal name.  Age: 2708+/-5Ma (SHRIMP).  Geological Province: Yilgarn Craton.||||||07-NOV-08
81730|Boreas suite''|71270|5|Briefly described|118947.1.pdf|||Geological province: Yilgarn Craton, West Australian Craton. Sample GSWA 118947 (porphyritic monzogranite) yielded a weighted mean 207Pb/206Pb date of 2637+\-8 Ma, interpreted as the crystallisation age of the monzogranite, and an interpreted metamorphic age of 2612+\-10 Ma. Sampled May 1995,Reported 1997.||||||22-NOV-19
42072|Borefield Road Suite|23809|5|Briefly described|p3 Fig. 1|||Includes the Nova Range monzogranite.  See also p5 Tb. 2.||||||26-JUL-06
42072|Borefield Road Suite|61861|6|Mentioned|Map 1|Paleoproterozoic|Paleoproterozoic|Mis-spelling of Borefield Road Igneous Complex? See also p4, p26.||||||03-APR-12
42072|Borefield Road Suite|62580|4|Described|p62|Proterozoic|Proterozoic|See also Borefield Road Complex - names used interchangeably. Circular composite intrusion NNE of The Granites. Medium- to coarse-grained, cumulate and subophitic textures. See also p71.||||||18-FEB-13
42072|Borefield Road Suite|64675|6|Mentioned|Map 1|Paleoproterozoic|Paleoproterozoic|||||||
40072|Bossut Formation""|24541|5|Briefly described|p63|Quaternary|Quaternary|Previously referred to locally as 'Bossut Formation'.||||||
42470|Boston Creek ferropicritic basalt|60696|6|Mentioned|p350|||Informal name.||||||
34473|Bow Hill dyke suite|22754|5|Briefly described|p22|||Informal term for suite of lamprophyres. Emplaced in granitoids of the Paperbark supersuite.||||||
32786|Bow Hill lamprophyre dykes|44230|5|Briefly described|Map Legend||Proterozoic|||||||
68080|Bow Hill lamprophyres|24568|5|Briefly described|p173|Neoproterozoic|Neoproterozoic|Informal name.  Age: ca. 815Ma.||||||06-APR-05
74121|Bow River Batholith|24197|6|Mentioned|p23|||Superseded by and incorporated into the Paperbark Supersuite.||||||07-FEB-11
80091|Bow River Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Paleoproterozoic|Paleoproterozoic|East Kimberley. Age ranges from 2500-1600 Ma [not particularly useful]||||||
80091|Bow River Dolerite Suite|71267|6|Mentioned|2_5m_interpdykel15_lut.csv|Paleoproterozoic|Paleoproterozoic|Events: Western Australian events (4000-0.01 Ma).|2500-1600 Ma (inferred)||||Dolerite dyke|
39432|Bow River Granite""|22754|6|Mentioned|p6|||Former collective name for most of the granitoids in the Halls Creek Orogeny.||||||
39432|Bow River Granite""|66845|6|Mentioned|p538|||Of Dow and Gemuts (1969). Roughly equivalent to Bow River batholith, although this paper also includes granites from Hooper Complex, and tonalite intrusions along eastern margin of Central zone. See also Bow River Granitoid Suite"".||||||
78626|Bow River Granitoid Suite""|66845|6|Mentioned|p538|||Of Ogasawara (1988). Roughly equivalent to Bow River batholith, although this paper also includes granites from Hooper Complex, and tonalite intrusions along eastern margin of Central zone in the batholith. See also Bow River Granite"".||||||17-FEB-14
34453|Bow River batholith|66845|4|Described|p535, p536, p537, p538, p539 Tb.1, p543|Paleoproterozoic|Paleoproterozoic|Single episode of high-K granite plutons (Hancock & Rutland, 1984; Page & Hancock, 1988), now shown as a complex intrusion history consistent with more recent plate tectonic models for the Lamboo Complex (Sheppard et al. 1999, Tyler et al. 1999; Griffin et al. 2000). SHRIMP U-Pb zircon dating and regional mapping has subdivided this unit into supersuites and suites. Most granites of the Lamboo Complex are part of this unit which is >750 km long and ~60-70 km wide. Divided into 2 supersuites.|1865-1805 Ma||Paperbark supersuite and Sally Downs supersuite||I-type granite and coeval gabbro|
72892|Bow batholith granitoids|60724|6|Mentioned|p21|||Informal name - see Bow River Granite.||||||
79637|Boyagin Dolerite Suite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province. Dyke.|1218-1202 Ma inferred|Marnda Moorn Supersuite.|||Dolerite.|
79637|Boyagin Dolerite Suite|70796|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Part of the Marnda Moorn Large Igneous Province. Mapping code is:P_MMBod. Also appears the Boyagin Dyke Suite in file: 2_5m_interpdykel15_lut.csv.|ca 1218 to 1202 Ma (inferred)|Marnda Moorn Supersuite|||Dolerite dyke|
79637|Boyagin Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Ectasian|Ectasian|West Yilgarn Craton.|1218-1202 Ma|||||
79637|Boyagin Dolerite Suite|71269|5|Briefly described|2_5m_interpdykel15_lut|Mesoproterozoic|Mesoproterozoic||1218-1202 Ma (inferred)||||Dolerite dyke|
29783|Boyagin Dyke Swarm|43038|5|Briefly described|p10|||||||||
29783|Boyagin Dyke Swarm|43560|6|Mentioned|fig.1,p227|||||||||
29783|Boyagin Dyke Swarm|62428|6|Mentioned|p343 Fig. 5|||||||||
83039|Boyagin dyke swarm|73184|6|Mentioned|p196|Ediacaran|Ediacaran|Potential source of Neoproterozoic-Cambrian detrital zircons in the Grant Group. [May be informal name?]|578-548 Ma|||||
78599|Boyagin dykes|65487|6|Mentioned|p9|||c1210 Ma, part of the Marnda Moorn Large Igneous Province, same trend as Beenong Dyke Suite but probably older (from cross-cutting relationships).||||||
78599|Boyagin dykes|68186|5|Briefly described|p31|||Part of the Marnda Moorn Large Igneous Province. Has the same (NW) trend as the Beenong Dyke Suite but is probably older.|c.1210 Ma.|||||
72480|Brady Well monzogranite|62107|6|Mentioned|p1391 Fig. 2|||Informal name. In the Eastern Goldfields Province.||||||
25808|Braeside Tillite|22801|6|Mentioned|P11||Permian|Equivalent to Paterson Formation||||||
25808|Braeside Tillite|29845|6|Mentioned|Plate 3|||||||||
25808|Braeside Tillite|30110|6|Mentioned|p81|||Sakmarian age.||||||
25808|Braeside Tillite|30340|6|Mentioned|p2533|||||||||
25808|Braeside Tillite|30341|4|Described|p145|||||||||
25808|Braeside Tillite|30503|6|Mentioned|p10|||Also mention Table 1||||||
25808|Braeside Tillite|32648|6|Mentioned|p32|||L.Perm.||||||
25808|Braeside Tillite|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
25808|Braeside Tillite|35226|6|Mentioned|p9|||Refers WAPET(1966).||||||
25808|Braeside Tillite|36890|3|Fully described|p343|||||||||
25808|Braeside Tillite|37106|6|Mentioned|Fig.2|||||||||
25808|Braeside Tillite|37212|6|Mentioned|p17|||||||||
25808|Braeside Tillite|42547|6|Mentioned|p97|||||||||
25808|Braeside Tillite|43876|14|Not recorded|p573||Sakmarian|Spelt 'tillite' on reference card.||||||
25808|Braeside Tillite|44297|14|Not recorded|p.5,14|||(F51-9).||||||
25808|Braeside Tillite|44298|14|Not recorded|map legend||Permian|||||||
25808|Braeside Tillite|44479|2|Defined|p.4,8,9,10|||E/51-1. Fluvioglacial deposits, varves. Time equivalent: Paterson Formation (Paterson Sheet), Grant Formation (Fitzroy Basin), Lyons Group (Carnarvon Basin).||||||
25808|Braeside Tillite|44480|14|Not recorded|map legend||Permian|||||||
25808|Braeside Tillite|44499|14|Not recorded|opp.p.6, Tb.1||Permian|||||||
25808|Braeside Tillite|44994|6|Mentioned|Fig.7|||Perm. Correlation.||||||
25808|Braeside Tillite|44998|2|Defined|p.67,78,102,104-246|Sakmarian|Stephanian|On many pages. p.67,78,102,104,124-5,-7,198,242,-6. Overlain by Oakover Beds & Callawa Formation. Sakmar.-Stephan.||||||
25808|Braeside Tillite|45016|14|Not recorded|p.18|||Glaciation.||||||
25808|Braeside Tillite|45153|2|Defined|App.4-65|early Sakmarian|early Sakmarian|||||||
25808|Braeside Tillite|45923|4|Described|p.66,70,72,73,77|||Tb.VI. map. (F51-5). Permian?||||||
25808|Braeside Tillite|45965|14|Not recorded|p.60|||||||||
25808|Braeside Tillite|48826|14|Not recorded|Tb.III|||Correlates with Grant Formation.||||||
25808|Braeside Tillite|48842|14|Not recorded|Tb.I|||||||||
25808|Braeside Tillite|66949|4|Described|p9, p13, p51 Appx.2, p58 Appx.3|||Clapp, 1925; Traves et al., 1956. Abandoned; considered part of Paterson Formation (Crowe and Turner, 1976). Type section detailed. Available core detailed.||Formerly of Grant Group.|||Mudstone, sandstone and diamictite.|30-OCT-15
25808|Braeside Tillite|68902|6|Mentioned|p9|||Abandoned name, for rocks in the Oakover Valley, subsequently included in the Paterson Formation.||||||
83334|Braeside Tillite''|73117|6|Mentioned|p26|||A now-informal unit incorporated in the Paterson Formation.||||||
83072|Breakaway Well Granodiorite|73151|6|Mentioned|p4|Neoarchean|Neoarchean|Yilgarn Craton. Age from Fletcher et al., (2001).|2655 +/- 4 Ma|||||
83072|Breakaway Well Granodiorite|73596|6|Mentioned|p1154|||Agnew-Wiluna Greenstone Belt. Inherited zircon aged 2850 +/- 5 Ma.||||||
32620|Bremer Range Metamorphics|44316|14|Not recorded|map legend||Archean|||||||07-NOV-08
32620|Bremer Range Metamorphics|46311|14|Not recorded|p.7,11,15,16||Archean|Of many pages. opp. p.6; map. (Archaean).||||||07-NOV-08
75795|Bresnahan Formation|24607|6|Mentioned|p969 Fig.2|||Unconformably overlies Capricorn Group. See also Bresnahan Group.||||||
24197|Bridget Adamellite|24025|5|Briefly described|p14|||Geological Province: Mosquito Creek Basin.||||||
24197|Bridget Adamellite|24197|5|Briefly described|p109|Paleoproterozoic|Paleoproterozoic|Of the Bridget Suite. Age: ~1731+/-10Ma. Geological province: Pilbara Block.||||||07-FEB-11
24197|Bridget Adamellite|38763|6|Mentioned|p103|||||||||
24197|Bridget Adamellite|39426|2|Defined|Table 1|Proterozoic|Proterozoic|||||||
24197|Bridget Adamellite|39697|6|Mentioned|p134|||||||||
24197|Bridget Adamellite|41592|6|Mentioned|p8|||||||||
24197|Bridget Adamellite|50435|6|Mentioned|p2.1|||Geological Province: Kimberley Block. Of the Bridget Suite.||||||
24197|Bridget Adamellite|63441|5|Briefly described|p13 tb. 2|Archean|Archean|Superseded by Bridget Suite. Geological province: Pilbara Craton.||||||07-FEB-11
24197|Bridget Adamellite|65008|6|Mentioned|p25|||Replaced by the Bridget Suite (Budd et al., 2002).||||||
24197|Bridget Adamellite|65827|6|Mentioned|p42|Statherian|Paleoproterozoic|Former name of Bridget Suite.
||||||
24197|Bridget Adamellite|66217|5|Briefly described|p55.|Proterozoic|Proterozoic|Of Hickman (1978); subsequently extended to Bridget Suite (Budd et al. 2002). A discordant, rectangular-shaped stock NE of Bridget Creek-Nullagine River confluence.||||||10-JUN-20
23417|Brigadier Beds|36112|5|Briefly described|p29|||||||||
23417|Brigadier Beds|41444|4|Described|p181|||||||||
23417|Brigadier Beds|42615|6|Mentioned|p27|||Superseded by Brigadier Formation.||||||
81373|Brilliant Ultramafic|70326|4|Described|p360,363|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Lindsay Basalt. Underlain by Burbanks Basalt. Correlable to Songvang Basalt. Intruded by Greenmont Sill.|Basaltic komatiite.|
81373|Brilliant Ultramafic|73391|6|Mentioned|p194, 244, Appendices.|||Standing and Castleden (2002). Regional stratigraphic correlation chart of other workers. Coolgardie Domain, Kalgoorlie Terrane.||||Overlies Burbanks Basalt. Is overlain by Lindsays Basalt.||
31937|Bringo shale|43876|14|Not recorded|p581||Middle Jurassic|||||||
39744|Broadhurst Formation, Lower|24194|6|Mentioned|p901 Tb.1|||Informal name - see Broadhurst Formation. Geological Province: Paterson Orogeny||||||
39743|Broadhurst Formation, Middle|24194|6|Mentioned|p901 Tb.1|||Informal name - see Broadhurst Formation. Geological Province: Paterson Orogeny||||||
39742|Broadhurst Formation, Upper|24194|6|Mentioned|p901 Tb.1|||Informal name - see Broadhurst Formation. Geological Province: Paterson Orogeny||||||
40498|Broadhurst Formation, upper|23900|6|Mentioned|p1535|Proterozoic|Proterozoic|Informal name - see Broadhurst Formation. Geological Province: Paterson orogen||||||
77571|Brock Conglomerate|66937|5|Briefly described|p166, pp172-175.|Archean|Archean|Lower part of the Brock Supersequence. 740 m thick.||Unit in Brock Supersequence.|||Matrix- and clast-rich cobble conglomerate; clasts rounded to well-rounded from pebbles to rare boulders, mainly of porphyritic rhyolite-dacite and basalt.|01-NOV-12
77572|Brock Sandstone|66937|5|Briefly described|p166, pp172-175.|Archean|Archean|Highly deformed, upper part of the Brock Supersequence. Hosts Thets Fault, a zone of intense flattening.||Unit in Brock Supersequence.|||Pebbly, massive to plane-bedded coarse-grained sandstone; rhythmically interlaminated sets of sandstone, siltstone and green shale, toppped by bedded chert.|01-NOV-12
77560|Brock Supersequence|66937|5|Briefly described|p155, pp172-175.|Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin. 1300 m thick.|||Includes Brock Conglomerate and Brock Sandstone.|Unconformably overlies White Hills Supersequence and Laverton Sequence. Is overlain by Wallaby Conglomerate.|Interbedded conglomerate, sandstone and shale.|
77560|Brock Supersequence|66938|6|Mentioned|p188.|Archean|Archean|||||||
77561|Brock-Wallaby Supersequence|66938|6|Mentioned|p187. |Archean|Archean|This name is presumably meant to be shorthand for "Brock and Wallaby Supersequences" (q.v.); the apparent interchangeability in this article of the terms Supersequence and basin adds to the confusion.||||||
78448|Brockman Creek Kimberlite|65827|5|Briefly described|p41-42|Orosirian|Orosirian|ENE-trending dyke. Intrudes Fig Tree Gneiss; Ar/Ar date of 1867+/-8 Ma (White, 2000). Spinel- and phlogopite-bearing hypabyssal-facies kimberlite.||||||
78448|Brockman Creek Kimberlite|75075|6|Mentioned|p419, 424|Paleoproterozoic|Paleoproterozoic|Marble Bar area, eastern Pilbara. Considered a possible source of alluvial diamonds at Nullagine.|c.1900 Ma.|||||
80622|Brockman Iron Formation""|71785|6|Mentioned|p89|||Usage by Campana et al 1964, as Dales Gorge Mb.||||||
77173|Brockman Iron Formations|67829|5|Briefly described|p448.|||[Formal name is singular]. Written also as Brockman IF (p452, p453). See also reference to Brockman BIF (p447). Contains vast tonnages of goethite-rich leached M-G ores. Contains roughly equal SiO2 (as chert) and iron oxide (mainly magnetite with subordinate hematite).||||||
76799|Brockman Iron-formation|64725|5|Briefly described|p58.|||Economically important iron ore host.||Unit in Hamersley Group.|Consists of Dales Gorge Member, Whaleback Shale Member and Joffre Member.|Overlies Mount McRae Shale. Is overlain by Weeli Wolli Formation.||
33840|Brockman Supersequence|22546|6|Mentioned|374|||Compared with Turee Creek Supersequence.||||||
33840|Brockman Supersequence|22682|5|Briefly described|Fig20,p29|Siderian|Archean|2590-2499 Ma. Hamersley Province. Now described as Carrawine and Lacuna Supersequences||||||07-NOV-08
33840|Brockman Supersequence|70254|5|Briefly described|p379|Paleoproterozoic|Paleoproterozoic|Depositional age fom Trendall et al., 1990, and coincides with formation of the Hamersley banded iron formations and periods on mantle plume activity (Barley et al., 1997; Isley and Abbott, 1999).|2470+\-4 Ma|||||
33840|Brockman Supersequence|72569|6|Mentioned|p21|||Of the Hamersley Basin. Potentially influenced by the same bottom current responsible for the alternating sand and mud beds in the Paraburdoo Member.||||||
69380|Bronzewing basalt|60980|5|Briefly described|p142 Fig.2, p144|||Informal name.||||||27-JUN-05
32732|Broome Buchia Beds|44998|3|Fully described|p.146-8||Tithonian|Informal Name. Correlated with Jarlemai Silstone. Probably m.Tithonian. older than Langey Beds. Overlain by Broome Sandstone. On many pages.||||||
39657|Broome Formation|24449|5|Briefly described|p741 Fig. 2|Neocomian|Neocomian|Age: ~125m.y.  Geological Province: Canning Basin.||||||
24769|Broome buchia beds|45153|6|Mentioned|App.6-101|||||||||
40107|Brown Formation|24161|6|Mentioned|p12 Fig.8|||Misspelt - see Browne Formation.||||||
70759|Brown Range Siltstone''|62453|6|Mentioned|p17|||Informal name.||||||
83172|Brown beds|73392|6|Mentioned|p4||||||||[probable misspelling of Browne beds, Browne Formation] Sampled from core of Yowalga 3 well.|
70760|Browne Beds''|62453|6|Mentioned|p19|||Informal name.||||||
70763|Browne Evaporites|62453|6|Mentioned|p18|||Superseded by Browne Formation||||||
70764|Browne Evaporites''|62453|6|Mentioned|p19|||Informal name.||||||
70740|Browne Formation, lower|62453|6|Mentioned|p21|||Informal name.||||||
70725|Browne Formation, upper|62453|6|Mentioned|p19|||Informal name.||||||
70761|Browne beds''|62453|6|Mentioned|p19|||Informal name.||||||
34887|Brownrigg Formation|22907|6|Mentioned|41|||||||||
34887|Brownrigg Formation|62453|5|Briefly described|p5 Fig. 3|Cryogenian|Cryogenian|Geological Province: Paterson Orogen.||||||
34887|Brownrigg Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological Province: Officer Basin (Centralian Superbasin). Moderately to well-sorted, fine- to coarse-grained sandstone.||||||22-APR-16
34887|Brownrigg Formation|67202|5|Briefly described|p117, p125|Neoproterozoic|Neoproterozoic|Conductance image. See also Brownrigg Sandstone (p64-65).||Tarcunyah Group.||||
34887|Brownrigg Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
34887|Brownrigg Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
34154|Browns Range Dome|22446|5|Briefly described|p19||Archean|||||||07-NOV-08
34154|Browns Range Dome|61056|6|Mentioned|p778 Fig. 1a, p785|||Term used in a structural context. Age: 2504+/-4Ma.||||||09-MAY-05
30720|Browns Range Dome Granite|23809|5|Briefly described|p7-8, p6 Tb. 3|Paleoproterozoic|Paleoproterozoic|Porphyritic granite.  Age: 1805+/-7Ma, 1796+/-7Ma and 1780+/-33Ma.||||||07-NOV-08
30720|Browns Range Dome Granite|64662|5|Briefly described|p46|Orosirian|Orosirian|Also informally named Browns Range Dome granite. Reinterpretation of zircon dating suggests younger Paleoproterozoic emplacement age: 1874+/-10Ma. Archean zircons now believed to be inherited. Detailed explanation (p46-7).||||||07-FEB-11
30720|Browns Range Dome Granite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1796+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
42074|Browns Range Dome granite|23809|6|Mentioned|p9-10 Figs. 6,7,8|Paleoproterozoic|Paleoproterozoic|Informal - see Browns Range Dome Granite.  Age: 1805+/-7Ma (Pb-Pb).||||||07-NOV-08
42074|Browns Range Dome granite|71349|5|Briefly described|p724-725, p736|Paleoproterozoic|Paleoproterozoic|Tanami Region. Informal name, but presented in Fig.1 as BRD Granite. A 1 to 3km-thick, largely granitic body forms the core of an E-W trending, ~60km by ~30km structure.|1870 Ma (Cross and Crispe, 2007).|||Is overlain by Pargee Sandstone and Birrindudu Group.||
42075|Browns Range Dome porphyritic granite|23809|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Informal - see Browns Range Dome Granite.  Age: 1805+/-7Ma.||||||07-NOV-08
35720|Browns Range Suite|50589|5|Briefly described|p1.4, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1882 +/- 14Ma. Geological Province: Granites-Tanami Block.||||||07-NOV-08
81272|Browns Range dome granite|72071|6|Mentioned|p1299|Orosirian|Orosirian|Intrudes Browns Range Metamorphics.|ca. 1.88 Ga|||||
42076|Browns Range intrusives|23809|5|Briefly described|p5 Tb. 2|Paleoproterozoic|Paleoproterozoic|Informal name - probably intended as B.R. Granite. Of the Coomarie Suite.  Age: 1805+/-7Ma.||||||25-NOV-08
79179|Bruno Member|65757|6|Mentioned|p81 Tb.2|||banded iron formation||||||
81727|Bryah Group, lower|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Bryah Basin, Capricorn Orogen. Affected by the following events: Capricorn Orogeny (1817  1772 Ma); Glenburgh Orogeny (2002  1947 Ma). See also 500k_interpgeop14_lut.csv.|ca 20141920 (inferred)|Bryah Group|Includes the Trillbar Formation and the Narracoota Formation.||Basalt, and felsic volcanic, ultramafic, and siliciclastic sedimentary rocks|
81727|Bryah Group, lower|71269|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin.|2014-1920 Ma (inferred)||||Basalt, and felsic volcanic, ultramafic, and siliciclastic sedimentary rocks|
81728|Bryah Group, upper|70796|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Bryah Basin, Capricorn Orogen. Affected by the following events: Capricorn Orogeny (1817  1772 Ma); Glenburgh Orogeny (2002  1947 Ma). See also 500k_interpgeop14_lut.csv.|ca 20141920 (inferred)|Bryah Group|Includes the Horseshoe Formation, Ravelstone Formation and Karalundi Formation.||Turbiditic sandstone and siltstone with minor ironformation|
81728|Bryah Group, upper|71269|4|Described|2_5m_interpgeop15_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Bryah Basin.|2014-1920 Ma (inferred)||||Turbiditic sandstone and siltstone with minor iron-formation|
33662|Bubble Member|44204|5|Briefly described|Map Legend||Proterozoic|Of Juderina Formation.||||||
33662|Bubble Member|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Unit shown in section only. Geol. Prov: Yerrida Basin.||Of Juderina Formation.|||Laminated stromatolitic carbonated beds, and dolostone.|14-APR-11
33662|Bubble Member|70796|6|Mentioned|Glengarry100_2645_stratig.pdf.|||Yerrida Basin.||Juderina Formation|||Stromatolitic chert and chert breccia.|
76071|Bubble Well member|65408|5|Briefly described|pp82-83.|Paleoproterozoic|Paleoproterozoic|Typo for Member.||Unit in Juderina Formation.|||Silicified evaporitic rocks and stromatolitic carbonate.
|18-NOV-11
23430|Buchanan Sandstone|40993|4|Described|p11|||||||||
23430|Buchanan Sandstone|41598|5|Briefly described|p412|||||||||
23430|Buchanan Sandstone|41840|2|Defined|p44|Devonian?||||||||
23430|Buchanan Sandstone|45047|6|Mentioned|p126|||See also P128.||||||
23430|Buchanan Sandstone|73255|6|Mentioned|p534 Fig.2|Devonian|Devonian|||Mahony Group||Disconformably overlies the Overland Sandstone, underlies the Glass Hill Sandstone.||
28407|Buchanan Sandstone""|41864|6|Mentioned|p57|||Replaced by Purralili Sandstone||||||
79810|Buddadoo Igneous Complex|69583|6|Mentioned|p49|Mesoarchean|Mesoarchean|Murchison Domain.||||||
79810|Buddadoo Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
79810|Buddadoo Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
79810|Buddadoo Igneous Complex|71168|5|Briefly described|p7|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.|c. 2800 Ma|Meeline Suite||||
70741|Buldya Group, lower|62453|6|Mentioned|p10|||Informal name. See Buldya Group.||||||
70741|Buldya Group, lower|62987|5|Briefly described|p30|||Informal - see Buldya Group. Geological Province: Officer Basin.||||||
70741|Buldya Group, lower|63022|6|Mentioned|p1015|||Informal - see Buldya Group. Contains major halite intervals. ||||||
70741|Buldya Group, lower|70793|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1000-800 Ma (inferred)|Unit of Buldya Group.|Includes Browne Formation, Lefroy Formation, Townsend Quartzite.||Siltstone, limestone, dolomite, sandstone, evaporites in subsurface and diapirs, basal sandstone; includes Townsend Quartzite, Lefroy Formation, and Browne Formation|
70741|Buldya Group, lower|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|1000-720 Ma||Includes Browne Formation, Lefroy Formation, Townsend Quartzite.||Siltstone, limestone, dolomite, sandstone, and evaporites in subsurface and diapirs; basal sandstone.|
70741|Buldya Group, lower|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).  See also Buldya Group, informal Buldya Group, upper.||Buldya Group|includes Townsend Quartzite, Lefroy Formation, and Browne Formation.||Siltstone, limestone, dolomite, sandstone, evaporites in subsurface and diapirs, basal sandstone.|
70748|Buldya Group, middle|62453|6|Mentioned|p10|||Informal name. See Buldya Group.||||||
70726|Buldya Group, upper|62453|6|Mentioned|p10|||Informal name. See Buldya Group.||||||
70726|Buldya Group, upper|63022|6|Mentioned|p1015|||Informal - see Buldya Group. ||||||
70726|Buldya Group, upper|70153|4|Described|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian||850 - 635 Ma (inferred).|Buldya Group|Includes Hussar Formation, Kanpa Formation,Steptoe Formation||Siltstone, sandstone, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic.|
70726|Buldya Group, upper|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_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|850-720 Ma (inferred0|Unit of Buldya Group.|Includes Hussar Formation, Kanpa Formation, Steptoe Formation.||Siltstone, sandstone, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic; includes Hussar, Kanpa, and Steptoe Formations|
70726|Buldya Group, upper|70802|5|Briefly described|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny; Paterson Orogeny; Petermann Orogeny.|850-635 Ma (inferred)||||Siltstone, sandstone, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic; includes Hussar, Kanpa, and Steptoe Formations|
70726|Buldya Group, upper|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|850-720 Ma||Includes Hussar Formation, Kanpa Formation, Steptoe Formation.||Siltstone, sandstone, dolomite, limestone, and evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic|
70726|Buldya Group, upper|71270|4|Described|500k_interpgeop16_lut.csv|Tonian|Tonian|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).|850-720 Ma (inferred)||Includes Hussar Formation, Kanpa Formation, Steptoe Formation.||Siltstone, sandstone, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic.|
70726|Buldya Group, upper|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).  See also Buldya Group, informal Buldya Group, lower.||Buldya Group|includes Hussar, Kanpa, and Steptoe Formations.||Siltstone, sandstone, dolomite, limestone, evaporites (halite, gypsum, anhydrite) in subsurface and diapirs; stromatolitic.|
40799|Bulgurri kimberlite, lower|23808|6|Mentioned|p15|||Informal name.||||||
26433|Bulka Hills Beds|22764|4|Described|Table1,p6||Adelaidean|250 m. Conformable on Landrigan Tillite.||||||01-FEB-10
26433|Bulka Hills Beds|35120|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26433|Bulka Hills Beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Kuniandi Group.|||Sublithic and lithic arenite, quartz arenite, conglomerate|
40764|Bulla Rocks monzogranite|24494|5|Briefly described|p21|||Informal - see Bulla Rocks Monzogranite. Intrudes the Murrin greenstone belt.||||||
35328|Bullgadoo Shale|23174|5|Briefly described|Fig5p8|Permian|Permian|Misspelling of Bulgadoo Shale.||||||
81295|Bullshead Supersuite|70020|6|Mentioned|p122,132|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton. HFSE-enriched granitic supersuite. May be geochemically similar to felsic rocks associated with VHMS mineralization.||||||
34558|Bunbury Basalts|64570|5|Briefly described|p852|Early Cretaceous|Early Cretaceous|Age: 123 and 130Ma (Ar-Ar). Geological Province: Perth Basin.||||||22-DEC-08
77707|Bunbury Casuarina basalts|60372|5|Briefly described|pp86-103.|||Erupted during separation of Greater India from southwestern margin of Australia. Geochemical data detailed in this study suggest no obvious continental contamination. The authors suggest an enriched mantle source, most likely the Kerguelen (Plateau) plume, with up to 30% depleted mantle material, for these rocks and the Rajmahal Group 1 basalts in India.|132 Ma (Frey et al, 1996)|||||06-FEB-18
77708|Bunbury Gosselin basalts|60372|5|Briefly described|pp86-103.|||Geochemical data detailed in this study suggest these rocks are highly contaminated. The authors suggest an enriched mantle source, most likely the Kerguelen (Plateau) plume, with contamination from the subcontinental mantle lithosphere.|123 Ma (Coffin et al, 2002)|||||06-FEB-18
73517|Bunbury Tholeiitic Suite|61045|6|Mentioned|p59|Mesozoic|Mesozoic|Age: 132-122Ma.||||||
24787|Bunbury basalt|23914|5|Briefly described|p161|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin.||||||
24787|Bunbury basalt|33747|6|Mentioned|p1072|||||||||
24787|Bunbury basalt|36019|6|Mentioned|Plate 9|||||||||
24787|Bunbury basalt|38231|6|Mentioned|p466|||||||||
24787|Bunbury basalt|40263|6|Mentioned|Table 2|||[Originally entered for NSW. CEBMar95]||||||
77706|Bunbury basalts|60372|5|Briefly described|pp84-103.|||Two episodes of continental flood eruptions: the Casuarina group at 132 Ma and Gosselin group at 123 Ma. The latter are more contaminated by continental material. Crops out in a fault graben between Yilgarn Craton and Leeuwin Complex. Isotope data for Hf, Re and Os are detailed.|132Ma (Frey 1996) ; 123 Ma (Coffin et al. 2002) .|||||06-FEB-18
77706|Bunbury basalts|65708|5|Briefly described|p98|Early Cretaceous|Early Cretaceous|Linked with the Kerguelen plume. Probably associated with the offshore Naturaliste Plateau.|130 Ma.||||Onshore basalt flows.|
35814|Bungle Bungle Dolomite ""|23314|6|Mentioned|336|||||||||
80092|Bungle Bungle Formation|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Osmond Basin.||||||
33968|Bungle Gap Limestone|22550|6|Mentioned|Fig 3|||||||||
39727|Bunjimah Pillow Member|24185|5|Briefly described|p746 Tb. 4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38999|Bunjinah formation|23870|6|Mentioned|p225|Paleoproterozoic|Paleoproterozoic|Informal - see Bunjinah Formation.  Age: 2070+/-114Ma (Rb-Sr) and 2063+/-245Ma (Pb-Pb).||||||07-NOV-08
40168|Bunker Bay Suite|24595|5|Briefly described|p588 Tb. 1|||Of Kay (1958).  Part of the Leeuwin Complex.  Later referred to as Cowaramup Gneiss by Myers (1994).  Geological Province: Leeuwin Block.||||||
81374|Burbanks Basalt|70326|4|Described|p360,362|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Burbanks Formation on p362.]||||Overlain by Brilliant Ultramafic. Correlated to Hickies Bore Basalt, Wongi Basalt.|Massive and pillowed basalt intercalated within mafic intrusions.|15-AUG-19
81374|Burbanks Basalt|73391|5|Briefly described|p194, 244, Appendices.|||Coolgardie Domain, Kalgoorlie Terrane. See Burbanks Formation (Appendices).||||Is overlain by Brilliant Ultramafic.||
81374|Burbanks Basalt|73596|6|Mentioned|p1159, 1161|||Coolgardie Inlier, Kalgoorlie Terrane.||||||
34353|Burnside Pluton|22737|5|Briefly described|10|||||||||
41361|Burnside Supersuite|50434|6|Mentioned|p3.2|||Informal. Included in Nornalup Supersuite.||||||10-FEB-14
32733|Burramundi Conglomerate|44366|14|Not recorded|p.20|||||||||
32733|Burramundi Conglomerate|44974|5|Briefly described|p35||Late Devonian|||||||
32733|Burramundi Conglomerate|44998|14|Not recorded|p26,43,46,47, map||Late Devonian|||||||
32733|Burramundi Conglomerate|66127|6|Mentioned|pp139-142.|||Of Guppy et al. (1958), after the Burramundi Range [now also spelt Barramundi and Burramundy]; subsequently the Barramundi Conglomerate (Griffin and Tyler, 1995; Tyler et al. 1998).||||||
83140|Burtville Group|72491|6|Mentioned|p5 Fig.4|||Burtville Terrane, Yilgarn Craton.||||||
78513|Burtville Sandstone|68107|4|Described|p608 Fig.4, p613, p616||Neoarchean|Standing (2008). Laverton Greenstone Belt, Burtville Terrane. Detrital zircon population dated at 2773 +/- 6 and 2771 +/- 4 Ma (Barley et al. 2006); intruded by Burtville granodiorite at 2716 +/- 4 Ma.||||Intruded by the Burtville granodiorite.|Comprises quartzose to feldspathic sandstone and lithic wacke.|22-SEP-14
78513|Burtville Sandstone|71168|6|Mentioned|p10|Neoarchean|Neoarchean|Burtville Terrane, Yilgarn Craton.|2777-2772 Ma|||||
78513|Burtville Sandstone|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Laverton Greenstone Belt, Burtville Terrane.|2772 +/- 7 Ma.|||Overlies Windarra Sandstone. Is overlain by Prendergast Shale.||
24800|Burvill beds|42994|6|Mentioned|p39|||||||||
24800|Burvill beds|45169|4|Described|p6|||||||||
24800|Burvill beds|47040|6|Mentioned|Fig.3|||||||||
24800|Burvill beds|60682|6|Mentioned|p25|||Superseded by Burvill Formation. Geological Province:Bonaparte Basin.||||||
24800|Burvill beds|69452|6|Mentioned|p36:16|||Jones (1984). Originally Burvill Beds (Veevers and Roberts, 1968); subsequently Burvill Formation (Cockbain, 1985).||||||12-JUL-16
81296|Butcher Bird granophyre|70020|6|Mentioned|p118,122|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.|2730+\-4 Ma|||||
31900|Butchers Gully Suite|24197|5|Briefly described|p85|Paleoproterozoic|Paleoproterozoic|I-(granodiorite) type. Intruded between 1865Ma and 1818Ma. Geological province: Kimberley Province.||||||07-FEB-11
31900|Butchers Gully Suite|50437|5|Briefly described|p1.7, 5.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma. Geological Province: Kimberley Region.  Interbedded with Olympio Formation.||||||07-NOV-08
31341|Butte Sandstone|43564|6|Mentioned|p453|||||||||
31341|Butte Sandstone|44657|14|Not recorded|p.11|||||||||
29433|Button beds|42933|5|Briefly described|Fig.94 p258|||Misspelling of Buttons Formation of Mory & Beere (1988).||||||
26443|Buttons Beds|23820|5|Briefly described|p203|Devonian|Devonian|Geological Province: Bonaparte Gulf Basin.||||||
26443|Buttons Beds|32648|6|Mentioned|p32|||Famennian||||||
26443|Buttons Beds|32664|6|Mentioned|Map legend|Late Devonian|Late Devonian|Briefly described in notes||||||
26443|Buttons Beds|32865|5|Briefly described|p468|||See also P70. Famennian. Fauna||||||
26443|Buttons Beds|32870|6|Mentioned|p45|||See also P48||||||
26443|Buttons Beds|33621|6|Mentioned|Table 1|||See also P181.||||||
26443|Buttons Beds|34085|6|Mentioned|Cor.chart|||Famennian||||||
26443|Buttons Beds|36890|3|Fully described|p378|||||||||
26443|Buttons Beds|36904|5|Briefly described|p9|||||||||
26443|Buttons Beds|44994|6|Mentioned|Fig.6|||Correlation||||||
26443|Buttons Beds|45038|2|Defined|p.59||Late Devonian|See also Figs & Plates.||||||
26443|Buttons Beds|45039|6|Mentioned|p1|||Upper Devonian. See also PP6,7,21,29 etc.||||||
26443|Buttons Beds|45040|14|Not recorded|p7||Late Devonian|See also p1,5,8,9,10,11,14,16,17,27,32,34,38,41,43,45,47,49,52,43,55,56,61,68,71, Fig.2,6,7. (Upper Devonian).||||||
26443|Buttons Beds|45041|6|Mentioned|Fig.45|||Famennian||||||
26443|Buttons Beds|45050|6|Mentioned|p9|||See also PP45,46,49 etc.||||||
26443|Buttons Beds|45056|6|Mentioned|p8|||Famen. Fig. 3||||||
26443|Buttons Beds|45063|6|Mentioned|p6|||See also P13, 24||||||
26443|Buttons Beds|45169|4|Described|p4|||||||||
26443|Buttons Beds|48886|14|Not recorded|Map. Fig.10||Late Devonian|Upper Devonian. Defn on Tech.File D/52-14.||||||
26443|Buttons Beds|48971|6|Mentioned|p10|||See also P13,17,18,20,21,24,27,29,30,31,36,37,42.||||||
26443|Buttons Beds|69452|6|Mentioned|p36:7, 10|||Veevers and Roberts (1968). Equivalent of Buttons beds of Playford (1982). Now the Buttons Formation (Mory and Beere, 1988).||||||12-JUL-16
33005|Byro Formation|44344|14|Not recorded|p.11|||(G50-1).||||||
42384|Byro Group Limestone""|23815|6|Mentioned|p283|||Superseded by the "Byro Formation" (Condit 1935). Geological Province: Carnarvon Basin.||||||
29627|Byro Limestone""|42994|6|Mentioned|p270|||||||||
32878|Byro Series|48848|14|Not recorded|p.51,52|||||||||
40315|C. halosa sand|50024|5|Briefly described|p13|Early Jurassic|Early Jurassic|Informal name.  A fault bound structure of the Athol Formation.  Hosts recoverable oil.  Geological Province: Carnarvon Basin.||||||
81615|Cada Formation|69029|6|Mentioned|p332|Bathonian|Aalenian|Of Perth Basin.||||Overlain by Yarragaddee Formation. Underlain by Cattamarra Coal Measures.||04-SEP-19
39303|Cadda Coal Measures|24374|5|Briefly described|p8|||Geological Province: Perth Basin.||||||
39303|Cadda Coal Measures|60118|6|Mentioned|p29|||Geological Province: Perth Basin||||||
28425|Caine's Well Granite|41250|6|Mentioned|Fig.1|||||||||
31674|Caines Well Granite Complex|22449|6|Mentioned|p28, Table3 p27||Archean|Age of emplacement is 3093 Ma for sample analysed. Also stated as 3090-2925 Ma. Shown as Caines Well Granitoid Complex in Table 3.||||||02-FEB-17
31674|Caines Well Granite Complex|24191|5|Briefly described|p828 Fig. 1|Archean|Archean|See also Caines Well Granite.  Age: 2925+/-4Ma (Nelson, 1997) and 3093+/-4Ma (Nelson, 1998).  Geological Province: Pilbara Craton.||||||07-NOV-08
31674|Caines Well Granite Complex|43821|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
31674|Caines Well Granite Complex|61267|6|Mentioned|p71|||Unconformably overlain by the Whim Creek Group.||||||
79303|Caines Well Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
69730|Caines Well Granitoid|24140|6|Mentioned|p214 Fig. 1|||Abbreviated version of Caines Well Granitoid Complex.||||||
69730|Caines Well Granitoid|24550|6|Mentioned|p39|Archean|Archean|In the Whim Creek Belt. Age: 3093+/-4 to 2990+/-5Ma.||||||07-FEB-11
35537|Caines Well Granitoid Complex|23244|5|Briefly described|Fig.2 p15,p23||Archean|Age: 2925Ma.||||||07-NOV-08
35537|Caines Well Granitoid Complex|23348|6|Mentioned|218|||||||||
35537|Caines Well Granitoid Complex|23484|6|Mentioned|p24|||||||||
35537|Caines Well Granitoid Complex|23783|5|Briefly described|p37 Tb. 1|Archean|Archean|||||||07-NOV-08
35537|Caines Well Granitoid Complex|23784|5|Briefly described|p20|Archean|Archean|Age: 3093+/-4Ma.||||||07-NOV-08
35537|Caines Well Granitoid Complex|23789|4|Described|p13|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
35537|Caines Well Granitoid Complex|23793|4|Described|p32|Archean|Archean|||||||07-NOV-08
35537|Caines Well Granitoid Complex|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province Pilbara Craton.||||||07-NOV-08
35537|Caines Well Granitoid Complex|23813|5|Briefly described|p99|Archean|Archean|Intrudes the Whundo Group.  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
35537|Caines Well Granitoid Complex|23936|5|Briefly described|Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 3093-2925 Ma.||||||07-NOV-08
35537|Caines Well Granitoid Complex|24023|6|Mentioned|p7 fig. 4|||||||||
35537|Caines Well Granitoid Complex|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||19-NOV-08
35537|Caines Well Granitoid Complex|24184|4|Described|p713, p715 Fig.12|Archean|Archean|Geological Province: Pilbara Craton. Main phase age: 2990 +/- 5Ma (Nelson 2000)||||||07-NOV-08
35537|Caines Well Granitoid Complex|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Age: ca. 3093-2925 Ma. Geological Province: Mallina basin||||||07-NOV-08
35537|Caines Well Granitoid Complex|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 3093-2925 Ma||||||07-NOV-08
35537|Caines Well Granitoid Complex|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Mallina Basin. Age: ca. 3095-2925 Ma||||||07-NOV-08
35537|Caines Well Granitoid Complex|24541|6|Mentioned|p45|||||||||
35537|Caines Well Granitoid Complex|24550|5|Briefly described|p39|Archean|Archean|See also Caines Well Granitoid. Intruded by Opaline Well and Sherlock Intrusions. Geological Province: Pilbara Craton. See also p79 Fig. 5.3.||||||07-FEB-11
35537|Caines Well Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||West Pilbara. Poorly exposed.|||||Foliated monzogranite, granodiorite, migmatite; some porphyritic phases.|
35537|Caines Well Granitoid Complex|50430|4|Described|p164||Archean|3016-2970 Ma. Derived from Whundo Group. In West Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
35537|Caines Well Granitoid Complex|60362|5|Briefly described|p1516-1517, p1518, p1525|Archean|Archean|Basement to NW Mallina Basin. Nd-isotopic data.|c.3.1 Ga and c.2.99 Ga.|||||
35537|Caines Well Granitoid Complex|67201|4|Described|p13 Fig.8, p19, p44, see comments|||In northwestern Pilbara Craton. Shown as Caines Well Granitic Complex p13, 19, 64. Source of granite boulders for coarse basal breccia of lower Warambie Basalt. Page location continued: p62 Fig.52, p63 Fig.54.|> 2990 Ma|||.||01-FEB-17
35537|Caines Well Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane. Isotopic ages: Nelson, 1997, 1997, and 2000, respectively.|2925 +/- 4 Ma, 3093 +/- 4, and 2990 +/- 5 Ma||||medium- to coarse-grained biotie monzogranite; metamorphosed. foliated biotite(-hornblende) monzogranite and strongly foliated to gneissic biotite tonalite to monzogranite; includes minor late biotite monzogranite|
40058|Caines Well Granitoid complex|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.3.12 Ga. Geological Province: Pilbara Craton. Informal - see Caines Well Granitoid Complex.||||||07-NOV-08
40058|Caines Well Granitoid complex|24140|6|Mentioned|p214 Fig. 1|||||||||
39733|Caines Well granitoid|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
29950|Cajuput dyke|43055|5|Briefly described|p12|||Trends north-northeast and has a maximum width of 1000 m, 2 km south of Daylight Rock Hole.||||Intrudes Mosquito Creek Formation, Kurrana Batholith. Unconformably overlain by Fortescue Group.|Gabbroic.|30-JAN-17
80623|Calamina Member|71785|14|Not recorded|p89|||Name abandoned.||||||
70228|Calcaling pegmatite|24410|6|Mentioned|p173 Fig. 110|||||||||
34524|Callawa Sandstone|22801|6|Mentioned|p13|||||||||14-JAN-20
80093|Callina Suite|70826|5|Briefly described|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Intrusion accompanied deposition of the Warrawoona Group.|||||Granites.|12-MAY-20
32852|Callytharra Limestone Group""|45016|14|Not recorded|p64||Permian|Ref to Dee & Rudd 1932 (unpubl). Permian.||||||
32761|Callytharra Stage""|45016|14|Not recorded|p.64|||Ref. to Raggatt 1936, Condit et al, 1936.||||||
37101|Calye Formation|23747|5|Briefly described|p16|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
31846|Calyerup Granodiorite|45003|6|Mentioned|p59|||See also Lexicon||||||
40742|Calyie Formation, upper|24183|6|Mentioned|p5|||Of the Collier Group.||||||
29690|Calytharra Formation|43018|5|Briefly described|Table 1 p386|||Misspelling of Callytharra Formation||||||
68978|Calytharra, Upper|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Informal. Geological Province: Carnarvon Basin.||||||
38128|Calytrix formation|23523|6|Mentioned|p994|||Informal - see Calytrix Formation. Of Grant Group.||||||
38128|Calytrix formation|69693|6|Mentioned|p4|||Shallow marine to lacustrine setting during a major deglaciation event.||||||
68609|Camel Hill Metamorphics|50216|5|Briefly described|p203, 210-211 Fig.4|Paleoproterozoic|Paleoproterozoic|Metasedimentary unit.||||||07-NOV-08
68609|Camel Hill Metamorphics|63866|4|Described|p157-p160|Paleoproterozoic|Paleoproterozoic|Outcrops extensively in the Erabiddy Shear Zone.|ca. 2025-1970 Ma||Includes the Petter Calc-silicate and the Quartpot Pelite.|Intruded by the Erong Granite.||
68609|Camel Hill Metamorphics|64161|6|Mentioned|p590, p591 Fig.11|Orosirian||Pre-1830 Ma metasedimentary rocks.||||||21-MAR-12
68609|Camel Hill Metamorphics|67247|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Glenburgh Terrane, Gascoyne Province.|2001 - 1955 Ma.||Includes Petter Calc-silicate and Quartpot Pelite.|||
68609|Camel Hill Metamorphics|69596|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Yilgarn Craton.||||||
68609|Camel Hill Metamorphics|72259|6|Mentioned|p3|Orosirian|Orosirian||ca. 2000-1955 Ma|||||
68609|Camel Hill Metamorphics|73168|6|Mentioned|p758|||Gascoyne Province.||||||
77180|Camp Sandstone|44139|6|Mentioned|p281 Table 3-15|||Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation.| | ||||10-SEP-12
39433|Camp shale member|22754|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Informal subdivision of Koongie Park Formation. Max. thickness: 300m.||||||07-NOV-08
38811|Campion dolerite|23931|6|Mentioned|p201 Table 1|||Informal name - see Campion Dolerite. Geological Province: Yilgarn Craton.||||||
38811|Campion dolerite|60979|5|Briefly described|p80 Fig.2, p90|||Part of the Jundee sequence - Jundee goldfield area. Medium-grained ophitic and cumulate - textured dolerite. Thickness: ~100-190. See also p91 Fig.4||||||27-JUN-05
40169|Canal Rocks|24595|6|Mentioned|p586 Fig.1b|||Informal name for part of the Leeuwin Complex.  See also p588.||||||
67861|Cane River supersequence""|24544|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|Informal. Of the Ashburton Formation (???). Geological Province: Ashburton Province.||||||07-NOV-08
34388|Cane River-Pingandy Supersequence|22682|5|Briefly described|Fig21,p31|Statherian|Orosirian|1815-1771 Ma. Ashburton Province||||||03-MAR-10
81602|Cangaroo Caves Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Misspelling of Kangaroo Caves Formation.||Unit of Sulphur Springs Group.||Uppermost unit of Sulphur Springs Group. Overlain unconformably by Budjan Creek Formation. Underlain by Kunagunarinna Formation.||11-FEB-20
81602|Cangaroo Caves Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane. [Mis-spelling of Kangaroo Caves Formation].||Sulphur Springs Group.||Overlies Kunagunarinna Formation. Is overlain unconformably by Budjan Creek Formation.||
83141|Cape Barren Group|72491|6|Mentioned|p2|Statherian|Statherian|Appears as Cape Barren Gp.||||||
74051|Cape Hay Formation, Lower|13242|6|Mentioned|p219|Late Permian|Late Permian|Informal - see Cape Hay Formation.||||||07-FEB-11
74052|Cape Hay Formation, upper|13242|6|Mentioned|p221|Late Permian|Late Permian|Informal - see Cape Hay Formation.||||||07-FEB-11
81147|Cape Riche beds""|71789|6|Mentioned|p100|||Name used by Maitland (1907) for what is now part of Pallinup Siltstone.||||||
40201|Capricorn Granites|24203|5|Briefly described|p292 Fig. 7|||Age: 1790 Ma.   Geological Province Carnarvon Basin.||||||
68610|Capricorn Group, lower|50216|5|Briefly described|p209|Paleoproterozoic|Paleoproterozoic|Age of lower Capricorn Group: ca. 1805 Ma (zircons). Geological Province: Blair Basin.||||||07-NOV-08
33931|Capricorn gneiss|22512|6|Mentioned|Fig1 P284|||||||||
33932|Capricorn granitoid|22512|6|Mentioned|Fig1 P284|||||||||
36131|Car Boyd Group|23516|6|Mentioned|p599 Fig.6|||||||||
24820|Carandibby Formation|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Of Lyons Group. Micaceous claystone,siltstone shale and sandstone.||||||28-OCT-09
24820|Carandibby Formation|46849|6|Mentioned|p195|||||||||
24821|Carawine Dolomite Series|36882|6|Mentioned|p124|||||||||
24821|Carawine Dolomite Series|39697|6|Mentioned|p125|||Refers Maitland 1919||||||
70201|Carawine Dolomite, lower|61575|6|Mentioned|p760, p761|||Informal - see Carawine Dolomite. ||||||
70202|Carawine Dolomite, upper|61575|6|Mentioned|p761|||Informal - see Carawine Dolomite. ||||||
70203|Carawine Impact Layer|61575|5|Briefly described|p766 Fig. 5|||Informal - see Carawine Dolomite - refers to the Carawine spherule layer. ||||||
41840|Carawine dolomite|50544|6|Mentioned|p72|||Informal - see Carawine Dolomite.||||||
70180|Carawine layer|61560|5|Briefly described|p498 Tb. 4|||Informal reference to Carawine Formation.||||||
70204|Carawine spherule layer|61575|3|Fully described|p762, p766|Neoarchean|Neoarchean|Informal - spherule layer within the Carawine Dolomite; interpreted as impact-generated melt. Age: 2548+26/29Ma. Thickness: 7.4m. Geol. Prov: Hamersley Basin.||||||07-NOV-08
70204|Carawine spherule layer|61576|5|Briefly described|p774 Fig. 1|Neoarchean|Neoarchean|Informal name - refers to impact spherule layer within the Carawine Formation. Age: 2548+26/-29Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
38966|Carbana Adamellite|69167|6|Mentioned|142978.1.pdf|Archaean|Archaean|Alternative name for Carbana Monzogranite (1983)||||||
38966|Carbana Adamellite|69590|6|Mentioned|142978.1.pdf|||Nomenclature of Hickman 1983. See Carbana Monzogranite.||||||
24211|Carbana Pool Adamellite|23807|5|Briefly described|p131|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
24211|Carbana Pool Adamellite|24590|5|Briefly described|p19, p40 Fig. 2.3|Archean|Archean|Rapakivi textured rock. Age: 3313+/-9Ma. See also p42, p43 Fig. 2.4b..||||||07-FEB-11
24211|Carbana Pool Adamellite|41636|6|Mentioned|p54|||||||||
24211|Carbana Pool Adamellite|44150|5|Briefly described|p146 Tb.2-21, p150 Fig.2-138|||200 sq. km. Post-tectonic granitoid.||Corunna Downs Granitoid Complex||Intruded by Mondana Adamellite.|Porphyritic biotite-hornblende monzogranite.|
24211|Carbana Pool Adamellite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Superseded by Carbana Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
24211|Carbana Pool Adamellite|64327|6|Mentioned|p63|Archean|Archean|Superseded by Carbana Monzogranite. Written as "Carbana Pool Adamellite".||||||07-NOV-08
81216|Carbana Suite|69041|4|Described|p10-p11, p18-p19|Paleoarchean|Paleoarchean|Pilbara Craton. Of the Corunna Downs Igneous Complex (used in the province sense). Extends across much of the northern, central and southern regions of the Complex. Outcrop ranges from isolated slabs in creeks and rivers to minor rubbly, very sparse scattered to abundant boulders and tors.Contains 13 unnamed sub-units. Mineralogy is provided. Monzogranite and granodiorite have relatively moderate radiometric total counts and low magnetic susceptibilities. Porphyry has a moderate radiometric total count and very low magnetic susceptibility.|3313 +/- 9 Ma (SHRIMP, Barley & Pickard, 1999)||||Fine- to coarse-grained, biotite monzogranite to biotite-hornblende monzogranite with minor porphyritic feldspar granite and biotite granodiorite. Rocks are seriate to granular and sparsely to moderately porphyritic and locally leucocratic.|21-JUN-19
42400|Carbunup Dune System|23816|6|Mentioned|p256|||Max. thickness: 18 m.||||||27-APR-05
26460|Cardabia Group|13615|4|Described|p4-p5, p20, 38, p101App.3|Eocene|Paleocene|Variation on Cardabia Calcarenite also used in this paper. Peedamullah Shelf. Spores/Pollen Zone and Dinoflagellate zones provided. Represents seismic section 10 of Westphal and Aigner.||||Disconformably overlies the Toolonga Calcilutite and the Gearle Siltstone. Unconformably overlain by the Trealla Limestone, Cape Range Group.||07-FEB-19
26460|Cardabia Group|23311|5|Briefly described|map legend|Eocene|Paleocene|||||||
26460|Cardabia Group|23403|6|Mentioned|p5|||Superseded by Cardabia Calcarenite.||||||
26460|Cardabia Group|23520|5|Briefly described|p6 Fig. 4|Eocene|Paleocene|Geological Province: Abrolhos Sub-basin.  See also p12.||||||
26460|Cardabia Group|23815|4|Described|p300|||Formerly known as the "Cardabia Series". Geological Province: Carnarvon Basin. Underlain by Miria Marl (disconformable). Overlain by Giralia Calcarenite (disconformable).||||||05-MAY-08
26460|Cardabia Group|24059|5|Briefly described|p132|Eocene|Paleocene|Geological Province: Barrow Sub-basin.||||||
26460|Cardabia Group|24084|5|Briefly described|p146 Fig.2|Paleocene|Paleocene|Geological Province: North Carnarvon Basin.||||||16-MAR-05
26460|Cardabia Group|24160|6|Mentioned|p37 Fig.12|Tertiary|Tertiary||||||Calcarenite.|
26460|Cardabia Group|29381|6|Mentioned|p67|||Appears on Table.||||||
26460|Cardabia Group|29721|6|Mentioned|p102|||||||||
26460|Cardabia Group|30304|5|Briefly described|p53|||Tertiary age||||||
26460|Cardabia Group|30875|6|Mentioned|p10|||Lower Eocene-Palaeocene. See also p13.||||||05-MAY-08
26460|Cardabia Group|31561|6|Mentioned|p34|||Marine. Eocene||||||
26460|Cardabia Group|32117|6|Mentioned|Fig.2|||||||||
26460|Cardabia Group|32166|6|Mentioned|p159|||||||||
26460|Cardabia Group|32648|6|Mentioned|p32|||Tertiary||||||
26460|Cardabia Group|32750|6|Mentioned|p301|||Tertiary. Stratigraphy||||||
26460|Cardabia Group|32752|6|Mentioned|Fig.5|||||||||
26460|Cardabia Group|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
26460|Cardabia Group|33386|6|Mentioned|Fig.7|||||||||
26460|Cardabia Group|33453|6|Mentioned|p72|||Palaeocene-Early Eocene.||||||
26460|Cardabia Group|33813|6|Mentioned|p7|||||||||
26460|Cardabia Group|34343|6|Mentioned|p96|||Formations||||||
26460|Cardabia Group|34363|6|Mentioned|p56|||Paleocene. See also p57, Figs 7and 8.||||||05-MAY-08
26460|Cardabia Group|34846|6|Mentioned|Fig.3|||||||||
26460|Cardabia Group|35105|6|Mentioned|Fig.5|||||||||
26460|Cardabia Group|35282|6|Mentioned|Fig.2|||||||||
26460|Cardabia Group|36257|6|Mentioned|Table 2.1|||||||||
26460|Cardabia Group|36305|6|Mentioned|p354|||||||||
26460|Cardabia Group|36890|3|Fully described|p300|||Formerly Cardabia Series.||||||05-MAY-08
26460|Cardabia Group|37016|6|Mentioned|Map legend|middle Eocene|Paleocene|Palaeocene to Middle Eocene||||||
26460|Cardabia Group|37320|6|Mentioned|p237|||||||||
26460|Cardabia Group|38485|4|Described|p17|||||||||
26460|Cardabia Group|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
26460|Cardabia Group|39427|6|Mentioned|p13|||||||||
26460|Cardabia Group|39486|6|Mentioned|Fig.2|||||||||
26460|Cardabia Group|40617|6|Mentioned|p14|||||||||
26460|Cardabia Group|41170|6|Mentioned|Fig.4|||||||||
26460|Cardabia Group|41172|6|Mentioned|p129|||||||||
26460|Cardabia Group|41443|6|Mentioned|Fig.3|||||||||
26460|Cardabia Group|41444|6|Mentioned|Fig.4|||||||||
26460|Cardabia Group|41447|6|Mentioned|Fig.3|||||||||
26460|Cardabia Group|41712|6|Mentioned|Fig.8|||||||||
26460|Cardabia Group|42123|6|Mentioned|Fig.8 P34|||||||||
26460|Cardabia Group|42995|5|Briefly described|Fig.8|||||||||
26460|Cardabia Group|43826|6|Mentioned|Fig.2,p163||Paleogene|||||||01-MAR-10
26460|Cardabia Group|44344|14|Not recorded|p.18, opp.4, map|||Includes Korojon Calcarenite.||||||
26460|Cardabia Group|44537|14|Not recorded|map legend|Tertiary|Cretaceous|Cretaceous-Tertiary.||||||
26460|Cardabia Group|44657|14|Not recorded|p.12|||||||||
26460|Cardabia Group|45142|6|Mentioned|Fig.4|||||||||
26460|Cardabia Group|45153|6|Mentioned|App.10-151|||||||||
26460|Cardabia Group|46950|6|Mentioned|Fig.15|||||||||
26460|Cardabia Group|48610|14|Not recorded|p14|||Salt Marsh area.||||||
26460|Cardabia Group|48861|14|Not recorded|p.5|||Ref.Condon et al. 1956.||||||
26460|Cardabia Group|67200|6|Mentioned|p17 table 1, p53|||Thermal conductivity of 1.68 W/mK||||||
32907|Cardabia Series|48861|14|Not recorded|p.5|||Ref. Raggatt, 1936.||||||
24822|Cardiff Member|31911|6|Mentioned|p98|||||||||
24822|Cardiff Member|36257|6|Mentioned|Table 2.1|||||||||
24822|Cardiff Member|36265|5|Briefly described|Fig.3.26|Late Permian|Late Permian|Of the Collie Coal Measures. Geological province: Collie and Wilga Basins. See also p136.||||||14-NOV-08
24822|Cardiff Member|36890|3|Fully described|p423|||||||||
24822|Cardiff Member|37104|6|Mentioned|Fig.3|||||||||
24822|Cardiff Member|37105|5|Briefly described|p273|||||||||
24822|Cardiff Member|37577|6|Mentioned|p64|||||||||
24822|Cardiff Member|38936|6|Mentioned|p322|||||||||
24822|Cardiff Member|39159|6|Mentioned|p42|||||||||
24822|Cardiff Member|40359|6|Mentioned|Fig.3b|||||||||
24822|Cardiff Member|40794|5|Briefly described|Fig.2|||||||||
24822|Cardiff Member|41785|6|Mentioned|Fig.1|||||||||
24822|Cardiff Member|41984|5|Briefly described|Fig.2 P4|||||||||
24822|Cardiff Member|42183|6|Mentioned|p363|||||||||
24822|Cardiff Member|42309|6|Mentioned|p240|||||||||
24822|Cardiff Member|42711|5|Briefly described|p17 Tb. 1|Permian|Permian|Of Fairbridge (1952). Replaced by Upper or Cardiff Phase of Woolnough (1916). Replaced by Muja Member by Playford et al (1975); then Muja Coal Measuresof the Collie Group.||||||11-AUG-08
24822|Cardiff Member|43067|6|Mentioned|p112|||||||||
24822|Cardiff Member|43068|5|Briefly described|Table 2,p138|||of Collie Coal Measures||||||
24822|Cardiff Member|46849|6|Mentioned|Fig. 6|||||||||
24822|Cardiff Member|67861|5|Briefly described|p526 fig 4-171, p528 fig 4-172, p531|Permian|Permian|Collie Basin.[Database says this replaced by Muja Member]||Of Collie Coal Measures.||||
28436|Cardup Series""|36293|6|Mentioned|p71|||Refers Prider 1941.||||||
28436|Cardup Series""|36872|6|Mentioned|p77|||Renamed Cardup Group.||||||
24823|Cardup Shale""|36293|6|Mentioned|p71|||Refers McWhae and others 1958.||||||
24823|Cardup Shale""|36872|6|Mentioned|p77|||Renamed Cardup Group.||||||
28437|Cardup-Armadale Shale""|36293|6|Mentioned|p71|||Refers Esson 1927.||||||
28437|Cardup-Armadale Shale""|36872|6|Mentioned|p77|||Renamed Cardup Group.||||||
25833|Caribuddy Formation|24246|5|Briefly described|p11|||Overlies Nita Formation. Geological Province: Canning Basin.||||||
25833|Caribuddy Formation|35057|5|Briefly described|p301|||Misspelling of Carribuddy?||||||
25833|Caribuddy Formation|35903|6|Mentioned|p7|||Misspelling of Carribuddy?||||||
25833|Caribuddy Formation|45153|2|Defined|App.2-24|Devonian|Devonian|Prob. Devonian||||||
39724|Carlindi Granite|24185|5|Briefly described|p745 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
39724|Carlindi Granite|72064|5|Briefly described|p67, p76|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Emplaced into Warrawoona Group prior to regional erosion.| 3468+\-4 Ma (U-Pb Zircon)|||Intruded into Warrawonna Group.||28-JAN-20
38074|Carlindi Granitic Complex|24166|6|Mentioned|p7|||Probably misspelt - see Carlindi Granitoid Complex||||||
38074|Carlindi Granitic Complex|64405|5|Briefly described|p2 Fig. 1, p7|||||||||07-FEB-11
38074|Carlindi Granitic Complex|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Undivided granitic rock; metamorphosed.||||||18-DEC-12
38074|Carlindi Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
38074|Carlindi Granitic Complex|64747|6|Mentioned|p95 fig 2|||||||||
38074|Carlindi Granitic Complex|65827|6|Mentioned|p15, p16|||Granitic components contain inherited 3650-3550 Ma zircons indicative of ancient sialic crust; has a central c.3240 Ma intrusion.
||||||
38074|Carlindi Granitic Complex|66118|6|Mentioned|p146 Fig.1, p149|||Pilbara Craton. [not a stratigraphic term as it is used in the Pilbara area].|c. 3469 Ma||||Granitic.|26-MAY-20
38074|Carlindi Granitic Complex|66217|4|Described|p1-2, p6, p11, p24, p28, p35, p43, p47.|||See also Carlindi Granitoid Complex. Folded leucosome veins formed during D1 deformation at c.3467 Ma. 150 km long by 70 km wide. Outcrops as subdued, undulating topography. Separated from the Muccan Granitic Complex to the east by the Warralong greenstone belt of Pilbara Supergroup rocks.|||Includes rocks of Tambina, Cleland, Callina, Split Rock and Sisters Supersuites.|Intruded by dykes of Bamboo Creek Member (of Hardey Formation).|Gneissic tonalites, undeformed porphyritic monzogranites, strongly foliated and folded granitic rocks, foliated to weakly strained monzogranites, undeformed monzogranites and syenogranites.|10-JUN-20
38074|Carlindi Granitic Complex|67197|6|Mentioned|p3, p18, p52|||Not a stratigraphic name. East Pilbara Terrane. Appears as Carlindie Granitic Complex on p18. Includes Callina Supersuite as a component.||||||
38074|Carlindi Granitic Complex|67270|6|Mentioned|p3|Archean|Archean|||||||
38074|Carlindi Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
38074|Carlindi Granitic Complex|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton.||||Extensively intrudes Table Top Formation.||
38074|Carlindi Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
38074|Carlindi Granitic Complex|71137|6|Mentioned|p5|Archean|Archean|Intrusions were mostly between 3490-3225 Ma, but minor intrusions occurred between 2955-2830 Ma (van Kranendonk, 2010).|3490-2830 Ma (see Comments).|||Metamorphosed Kelly and Warrawoona Groups.||
33447|Carlindi Granitoid Complex|23416|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|23755|4|Described|p47|Archean|Archean|Age: 3469+/-2 Ma.||||||07-NOV-08
33447|Carlindi Granitoid Complex|23780|5|Briefly described|p126|Archean|Archean|||||||07-NOV-08
33447|Carlindi Granitoid Complex|23783|5|Briefly described|p18|Archean|Archean|||||||07-NOV-08
33447|Carlindi Granitoid Complex|23784|6|Mentioned|p45|||||||||
33447|Carlindi Granitoid Complex|23794|5|Briefly described|Map Legend|||||||||
33447|Carlindi Granitoid Complex|23813|5|Briefly described|p101|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33447|Carlindi Granitoid Complex|23895|5|Briefly described|p884 Fig.1|||Geological Province: Pilbara Craton.||||||07-MAR-05
33447|Carlindi Granitoid Complex|23936|6|Mentioned|p13|||Geological Province: Pilbara Craton.||||||
33447|Carlindi Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3484-2941Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
33447|Carlindi Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|24166|4|Described|p17|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|24184|4|Described|p699, p703|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.2935Ma. Intrudes the Coonterunah Group||||||07-NOV-08
33447|Carlindi Granitoid Complex|24327|5|Briefly described|Map Legend|Archean|Archean|Includes the Kadgewarrina, Poocatche and Minnamonica Monzogranites.  Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|24349|5|Briefly described|Map legend|Archean|Archean|Includes the Kadgewarrina, Poocatche and Minnamonica Mozogranites.   Age: c.2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|24550|6|Mentioned|p33|||Reference also made to the Carlindi Batholith (p121 Fig. 6.2).||||||07-FEB-11
33447|Carlindi Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p145 Tb.2-21, p152|||See also p153 Fig.2-140, p155 Fig.2-142. |||Includes Tabba Tabba Adamellite.||Monzogranites, syenogranite, granodiorite, diorite, tonalite, gneiss, greenstones.|
33447|Carlindi Granitoid Complex|50302|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33447|Carlindi Granitoid Complex|50379|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33447|Carlindi Granitoid Complex|50427|6|Mentioned|p182 Fig.5|Archean|Archean|||||||07-NOV-08
33447|Carlindi Granitoid Complex|61111|6|Mentioned|p96 Fig.2|||||||||
33447|Carlindi Granitoid Complex|61266|6|Mentioned|p56|||Intrudes the Coonterunah Group.||||||
33447|Carlindi Granitoid Complex|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Structural term. Geological Province: Pilbara Craton.||||||07-NOV-08
33447|Carlindi Granitoid Complex|64326|6|Mentioned|p71 Fig. 1|Archean|Archean|Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
33447|Carlindi Granitoid Complex|64747|6|Mentioned|p94 fig 1|||||||||
33447|Carlindi Granitoid Complex|64936|5|Briefly described|map legend|Archean|Archean|Fine grained granite, metamorphosed; biotite monzogranite; biotite monzogranite to granodiorite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
33447|Carlindi Granitoid Complex|66217|4|Described|p1, p2, p6 Table 1, p11. |Paleoarchean|Paleoarchean|Referred to as Carlindi Granitic Complex (p1, p2, p6, p11, p24, p28, p35, p43, p47). Folded leucosome veins formed during D1 deformation at c.3467 Ma. 150 km long by 70 km wide. Outcrops as subdued, undulating topography. Separated from the Muccan Granitic Complex to the east by the Warralong greenstone belt of Pilbara Supergroup rocks.|3469 Ma.||Includes rocks of Tambina, Cleland, Callina, Split Rock and Sisters Supersuites.|Intruded by Bamboo Creek Member (of Hardey Formation).|Gneissic tonalites, undeformed porphyritic monzogranites, strongly foliated and folded granitic rocks, foliated to weakly strained monzogranites, undeformed monzogranites and syenogranites.|
33447|Carlindi Granitoid Complex|69167|6|Mentioned|178031.1.pdf|Archaean|Archaean|(Structural?)Age derived from samples of  granodiorites (178031.1.pdf, 178040.1.pdf)|3250 +/- 2 Ma - 3252+/- 4 Ma   (SHRIMP)|||||
33447|Carlindi Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as 3485-2850 Ma; also of Kenny (2000).|3484+/-4 Ma (isotopic age, Nelson 1999)||||undivided tonalite to monzogranite; metamorphosed|
40183|Carlindi granitoid|24016|6|Mentioned|p295|||Informal name.||||||
39735|Carlindi granitoid complex|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
40157|Carlindi granitoids|24016|6|Mentioned|p294 Fig. 1|Archean|Archean|Informal name.||||||07-NOV-08
40157|Carlindi granitoids|24621|6|Mentioned|p74|Archean|Archean|Informal name.||||||07-NOV-08
40154|Carlindi granodiorite|24621|5|Briefly described|p78|Archean|Archean|Informal name.  Age: ~2760-2640Ma (Pb-Pb).  Intrudes the Coonterunah Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
39725|Carlindie Granitoid Complex|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Geological Province: Mallina basin||||||07-NOV-08
39725|Carlindie Granitoid Complex|24190|5|Briefly described|p820 Fig.1|Archean|Archean|||||||07-NOV-08
39725|Carlindie Granitoid Complex|50555|6|Mentioned|Map legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
78776|Carlson Volcanics|63458|6|Mentioned|p875 Fig.3.|||||||Is overlain unconformably by Walsh Tillite.||
28438|Carlton Series""|41864|6|Mentioned|p29|||||||||
23471|Carnac Formation""|40300|6|Mentioned|p1|||||||||
40802|Carnac Formation, Intra-|12758|6|Mentioned|p31 Fig. 32|||Informal name - see Carnac Formation.  Highly radioactive shale bed within the Carnac Formation.||||||
24825|Carnac Member|12758|5|Briefly described|p18, p20|Berriasian|Tithonian|Originally the Carnac Formation (WAPET), redefined as "Carnac Member" of the Parmelia Formation by Backhouse (1984). Now restored and upgraded to Carnac Formation of the Parmelia Group. Thickness in type section: 656m.  Geol. Prov: Vlaming Sub-basin.||||||
24825|Carnac Member|12759|6|Mentioned|p28-31 Tb.7,8|||||Unit in Parmelia Formation.|||Shale and siltstone.|09-MAY-14
24825|Carnac Member|23279|6|Mentioned|p30|||(Backhouse, 1984).||||||
24825|Carnac Member|40300|3|Fully described|p4|||||||||
24825|Carnac Member|41728|6|Mentioned|p444|||||||||
24825|Carnac Member|41989|6|Mentioned|p111|||||||||
24825|Carnac Member|42194|5|Briefly described|p5|||||||||
24825|Carnac Member|43031|5|Briefly described|Fig.2.|||of Parmelia Formation||||||
24825|Carnac Member|43096|6|Mentioned|p5|||of Parmelia Formation||||||
24825|Carnac Member|44144|6|Mentioned|p505 Tb.4-21, p515 fig 4-155, p516|Berriasian|Tithonian|Lacustrine sediments. Top fill for Perth basin rift valley.||Parmelia Formation|||Siltstone, shale.|
40800|Carnac Member""|12758|6|Mentioned|p20|||Informal name - see Carnac Member of the Parmelia Formation.  Now upgraded to Carnac Formation of the Parmelia Group.||||||
40806|Carnac Sandstone Sequence, Intra-""|12758|6|Mentioned|p18|||Informal reference to an economically significant subunit of the former Carnac Member.||||||
40807|Carnac Sandstone sequence, Intra-""|12758|6|Mentioned|p20|||Informal reference to an economically significant subunit of the former Carnac Member.  See also "Intra-Carnac Sandstone Sequence".||||||
40803|Carnac Sandstone,  Intra-""|12758|6|Mentioned|p46|||Of Devereux (1993).  A largely shaly lithostratigraphic portion of what is now the Carnac Formation.||||||
40805|Carnac Sandstone, Intra-|12758|6|Mentioned|p47 Fig. 50|||Informal name of Devereux (1993) in his lithostratigraphy of the Carnac Formation.  See also "Intra-Carnac Sandstone sequence".||||||
40804|Carnac Sandstone, Lower|12758|6|Mentioned|p47 Fig.50|||Informal name of Devereux (1993) in his lithostratigraphy of the Carnac Formation.||||||
40808|Carnac Sandstone, Lower""|12758|6|Mentioned|p46|||Informal name of Devereux (1993) in his lithostratigraphy of the Carnac Formation.  See also Lower Carnac Sandstone.||||||
34396|Carnegie/Boord Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
74721|Caroline Formation|64580|6|Mentioned|map legend|||Of Grant Group. Misspelling of Carolyn Formation.||||||
74721|Caroline Formation|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|||[Of Grant Group. Misspelling of Carolyn Formation.]||Grant Group||||25-NOV-15
74721|Caroline Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian|||||||
74721|Caroline Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Grant Group.||||
31103|Carpet Snake Monzogranite|43478|6|Mentioned|p31|||||||||
24826|Carr Boyd Rocks complex|41640|6|Mentioned|p17|||||||||
74722|Carrandiby Formation|64580|6|Mentioned|map legend|||Of Lyons Group. Misspelling of Carrandibby Formation.||||||
26463|Carranya Beds|22764|4|Described|Table2,p11||Early Ordovician|||||||01-FEB-10
26463|Carranya Beds|24061|5|Briefly described|p175|Early Ordovician|Early Ordovician|Of the Nambeet Formation.  Geological Province:  Canning Basin.||||||
26463|Carranya Beds|29813|6|Mentioned|p7|||||||||
26463|Carranya Beds|29818|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26463|Carranya Beds|33738|6|Mentioned|p47|||See also P57.||||||
26463|Carranya Beds|33962|6|Mentioned|p50|||||||||
26463|Carranya Beds|35119|4|Described|p459|||See also mention on P448.||||||
26463|Carranya Beds|35120|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
26463|Carranya Beds|36890|3|Fully described|p322|||||||||
26463|Carranya Beds|40136|5|Briefly described|p20|||||||||
26463|Carranya Beds|40866|6|Mentioned|p179|||||||||
26463|Carranya Beds|41215|6|Mentioned|Fig.5|||||||||
26463|Carranya Beds|41730|6|Mentioned|Fig.3|||||||||
26463|Carranya Beds|41854|6|Mentioned|p94|||||||||
26463|Carranya Beds|43563|6|Mentioned|p4||Ordovician|Should be Carranya Formation||||||
26463|Carranya Beds|43803|6|Mentioned|p65||Ordovician|||||||
26463|Carranya Beds|45140|5|Briefly described|p66-67|Ordovician|Ordovician|Oldest unit in the Canning Basin sequence.||||Unconformably overlies Baines Beds (onlaps) and (inferred) the Ima Ima Beds, Duerdin Group and Albert Edward Group. Is overlain unconformably by Knobby Sandstone.|Fossiliferous marine sandstone and conglomerate.|
80094|Carranya Sandstone|70826|6|Mentioned|p7 tbl 3|Silurian|Ordovician|Canning Basin.||||||
25835|Carranya beds|7433|5|Briefly described|p25 Fig.2, p28 Fig.5, p29. |Ordovician|Ordovician|Billiluna Shelf, Canning Basin. Grades laterally into finer-grained marine sediments.||||Grades laterally into Prices Creek Group.|Paralic, sparingly fossiliferous sandstones and conglomerates.|
25835|Carranya beds|38878|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
25835|Carranya beds|41854|6|Mentioned|Fig.2|||||||||
25835|Carranya beds|43173|6|Mentioned|54||Ordovician|||||||
25835|Carranya beds|43819|6|Mentioned|p31||Arenig|||||||
25835|Carranya beds|45153|2|Defined|App.1-18|Early Ordovician|Early Ordovician|See also App.1-2.||||||
25835|Carranya beds|45158|3|Fully described|p28|||||||||
25835|Carranya beds|62982|5|Briefly described|p7|Ordovician|Ordovician|Sparse sandstone and conglomerate outcrops. Overlain by Carribuddy Group. Geological Province: Canning Basin.||||||
34531|Carribuddy Formation equivalent|22764|4|Described|Table2,p11|Early Devonian|Late Ordovician|?2000||||||01-FEB-10
39656|Carribuddy group|24449|6|Mentioned|p748|||Informal - see Carribuddy Group.||||||
40307|Carribudy Group|24390|5|Briefly described|p6 Fig. 4|Silurian|Ordovician|Geological Province: Canning Basin.||||||
40307|Carribudy Group|50085|5|Briefly described|p6 Fig. 4|Silurian|Ordovician|Geological Province: Canning Basin.  See also reference to Carribuddy Formation (p8).||||||
77443|Carrynginia Formation|60386|6|Mentioned|p297|Kungurian|Kungurian|[Mis-spelling of Carynginia Formation] Northern Perth Basin. Deltaic - nearshore - shelf. See page 304 for Carynginia.||||||
78802|Carson Group|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|Presented as Carson Gp in figure. [Should be Carson Volcanics].||||||
69586|Cartier Formation""|61155|5|Briefly described|p15||Early Oligocene|Overlain by rocks of the "Fantome Formation". Max. thickness: 200m. Geological Province: Bonaparte Basin / Ashmore Platform.||||||
74140|Caryinginia Formation|60376|5|Briefly described|p17 Fig. 4.|Early Permian|Early Permian|Probably misspelt - correct place name is Carynginia. Geological Province: Perth Basin. Underlain by Irwin River Coal Measures. Unconformity at top of unit.||||||07-FEB-11
24828|Carynginia Formation sandstone|37703|6|Mentioned|p2243|||||||||
77198|Carynginia Shale|61811|6|Mentioned|p38.|Permian|Permian|Of Clarke et al. (1951); subsequently amended to Formation status by Playford and Willmott in McWhae et al. (1958).||||||
77198|Carynginia Shale|64635|6|Mentioned|p20|||Of Clarke et al. (1951); subsequently Carynginia Shale (Playford and Willmott in McWhae et al., 1958).||||||
26466|Cashin Calcarenite|23311|5|Briefly described|map legend|Eocene|Paleocene|of Cardabia Group.||||||
26466|Cashin Calcarenite|23815|4|Described|p300|Early Eocene|Paleocene|Geological Province: Carnarvon Basin. Of the Cardabia Group. Underlain by Pirie Calcarenite. Overlain by Jubilee Calcarenite. Max thickness: 14 m.||||||05-MAY-08
26466|Cashin Calcarenite|24059|5|Briefly described|p138|Tertiary|Tertiary|Geological Province: Exmouth Sub-basin.||||||
26466|Cashin Calcarenite|24094|5|Briefly described|p268, p276|Early Eocene|Late Paleocene|Of Cardabia Formation. Name used interchangably with Cashin Calcarenite Member. Overlies Pirie Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
26466|Cashin Calcarenite|32648|6|Mentioned|p32|||Cardabia Gp.||||||
26466|Cashin Calcarenite|34343|6|Mentioned|p96|||Middle Paleocene||||||
26466|Cashin Calcarenite|35105|6|Mentioned|Fig.64|||||||||
26466|Cashin Calcarenite|35282|6|Mentioned|p27|||||||||
26466|Cashin Calcarenite|36119|6|Mentioned|p50|||||||||
26466|Cashin Calcarenite|36257|6|Mentioned|Table 2.1|||||||||
26466|Cashin Calcarenite|36890|3|Fully described|p300|||||||||
26466|Cashin Calcarenite|37016|6|Mentioned|Map legend|middle Eocene|middle Eocene|||||||
26466|Cashin Calcarenite|39427|4|Described|Table 1|||||||||
26466|Cashin Calcarenite|44537|14|Not recorded|map legend|Tertiary|Cretaceous|Cretaceous-Tertiary.||||||
26466|Cashin Calcarenite|44657|14|Not recorded|p.5,6,12,13|||||||||
26466|Cashin Calcarenite|45015|5|Briefly described|map legend|Tertiary|Tertiary|Age is Early Tertiary. Geological Province: Carnarvon Basin.||||||31-MAY-06
26466|Cashin Calcarenite|61958|5|Briefly described|Map sheet 1|Paleogene|Paleogene|||||||
39252|Cashin Calcarenite Member|24094|5|Briefly described|p275|||Name used interchangably with Cashin Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
83350|Cashmans Complex|73391|6|Mentioned|Appendices.|||Witt (1990). Regional stratigraphic correlation chart of other workers.|||||Metasedimentary rocks, grey pyritic shale, bedded tuff, porphyry flow.|
42155|Cashmans Sedimentary Horizon|50551|5|Briefly described|p1094 Fig.5|||Intruded by Enterprise dolerite. In Eastern Goldfields Province.||||||24-NOV-04
78801|Castlereigh Hill Porphyry|64104|6|Mentioned|p76|||[Mis-spelling of Castlereagh]. Possible source of quartz-feldspar porphyry cobbles in Fargoo Formation.||||||
77573|Casuarina Stone|67135|6|Mentioned|p52.|||Local name for a diatomaceous clay, formerly used for buildings, with economic potential as a cut building stone.||||||
77709|Casuarina group|60372|5|Briefly described|pp86-103.|||Informal name for an early component of Bunbury Basalt. Continental flood basalt eruption at c.132 Ma  during separation of Greater India from southwestern margin of Australia.|132 Ma (Frey et al, 1996)|||||06-FEB-18
78585|Cattamara Coal Measures|69081|6|Mentioned|p739 Fig.2|||Presented as Cattamara C.M. in figure. Misspelling of Cattamarra Coal Measures. See Cattamarra Coal Measures.||||||
40184|Cattamarra Coal Measures Sandstone|23520|5|Briefly described|p32|Jurassic|Jurassic|Not intended as a formal name - the main productive interval for petroleum in the Cattamarra Coal Measures.  Also known as the "F sand".||||||
73766|Cattamarra Formation|24351|5|Briefly described|Plate 3 (in pocket)|Jurassic|Jurassic|Log Houtman-1. Name writeen as Cattamarra only.||||||23-JAN-08
38830|Cattamurra Coal Member|24058|5|Briefly described|p112|Early Jurassic|Early Jurassic|Of Cockleshell Gully Formation.  Geological Basin: Perth Basin.||||||
34795|Cattle Well Unit|22774|5|Briefly described|p572, Fig.2 p573|||See also Fig.3 p574||||||
69766|Cavanagh gabbro intrusion|61339|5|Briefly described|Map legend|||Flat-lying gabbro and gabbronorite intruded by a network of mafic dykes on a dense scale. Max. thickness: 100m.||||||
69742|Cavenagh Range Gabbro Intrusion|61341|5|Briefly described|Map legend|||Informal name.||||||
70168|Cavenagh Range gabbro|44109|6|Mentioned|p80|Mesoproterozoic|Mesoproterozoic|Informal reference to rocks of the Cavenagh Range intrusion. ||||||
70171|Cavenagh Range gabbro intrusion|44109|5|Briefly described|p10, p91|Mesoproterozoic|Mesoproterozoic|Informal name for part of the Giles Complex mafic-ultramafic intrusions. Consists of nearly flat-lying sheets of grabbro and gabbronorite cut by dense swarms of subvertical dolerite dykes.||||||
28072|Cavenagh gabbro|65693|5|Briefly described|p14.|||Incompatible trace elements detailed.||||||
78328|Cavenagh intrusion|65135|6|Mentioned|p14|||Informal name. Of the Giles intrusions.||||||
78328|Cavenagh intrusion|68996|5|Briefly described|p39-41, 50, 52, 63, 65, 67|Mesoproterozoic|Mesoproterozoic|See also Blackstone-Cavenagh intrusion p47.||Giles Suite||Along with Latitude Hills intrusion, characterised by very strong aeromagnetic anomalies. Connected at depth with Jameson, Blackstone and Bell Rock intrusions.||17-JAN-17
26470|Cecil Sandstone Member|32664|6|Mentioned|Map legend|Late Devonian|Late Devonian|Briefly described in notes||||||
26470|Cecil Sandstone Member|36890|4|Described|p376|||||||||
26470|Cecil Sandstone Member|45038|2|Defined|p.17,22,23,134||Late Devonian|See also Figures.||||||
26470|Cecil Sandstone Member|45040|14|Not recorded|p5, Fig.2||Late Devonian|(Upper Devonian). pt. Cockatoo Formation.||||||
26470|Cecil Sandstone Member|45050|6|Mentioned|p6|||See also P8.||||||
26470|Cecil Sandstone Member|45063|6|Mentioned|p6|||Devonian||||||
26470|Cecil Sandstone Member|48886|14|Not recorded|Map||Late Devonian|Upper Devonian||||||
80123|Cemetery Layered Mafic-Ultramafic Complex|71212|5|Briefly described|intro p2, p46, p55, p59, p89|||Yilgarn Craton. Informal name, equivalent to the formal Satellite Igneous Complex. Maximum thickness of up to 1500m. See also  p121, p128, p129, p198, p256. Shown as Cemetery layered mafic-ultramafic complex intro p2.||||||26-SEP-17
69192|Centenary Bore basalt|60514|6|Mentioned|p96 Fig. 2|Archean|Archean|Informal name. Geological Province: Yilgarn Craton.||||||07-FEB-11
69192|Centenary Bore basalt|60629|6|Mentioned|p96 Fig.2|||Informal.||||||
38588|Central Ultramafic|23782|6|Mentioned|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
38588|Central Ultramafic|60514|6|Mentioned|p94, p95, p96 Fig. 2|Archean|Archean|Geological Province: Yilgarn Craton. Basal accumulations of massive Ni-Fe sulfide at the base. Dips steeply to the west. Subaqueous intrusive sequence.||||||07-FEB-11
38588|Central Ultramafic|60628|5|Briefly described|p87, 90|||Contains well developed spinifex textured komatiites. Dips steeply to the west. Overlies Eastern Ultramafic. Local name.||||||
38588|Central Ultramafic|60629|5|Briefly described|p94 Fig.1, p95|||Dips steeply to the west. Local name. Overlies Eastern Ultramafic. See also Central Ultramafic unit.||||||
38593|Central Ultramafic Unit|23782|4|Described|p53|||Informal name.  Geological Province: Yilgarn Craton.||||||
38593|Central Ultramafic Unit|60628|6|Mentioned|p89 Fig.2|||Local name. See also Central Ultramafic.||||||
69191|Central Ultramafic unit|60629|5|Briefly described|p93-95|||Well developed spinifex textures. Dips steeply to the west. Subaqueous extrusives. Local name. See also Central Ultramafic.||||||
83351|Centurion Porphyry|73391|5|Briefly described|p100, 179, 350, 390, 392-397, 403-406|||See also p411-412, 414, 444. Binduli area, Ora Banda Domain. Intruded into faults active at the time of volcanism and deposition. Detailed description: photographs. Makes up the bulk of clasts in Binduli Porphyry Conglomerate.|2667 +/- 3 Ma (SHRIMP: Fletcher et al., 2001).|Part of the upper Black Flag Formation/Group.|||Mafic hypabyssal intrusion; a crowded biotite-hornblende feldspar-phyric, aphanitic-groundmass with rare quartz intrusion.|
40809|Charlotte Sandstone""|12758|6|Mentioned|p18|Neocomian|Neocomian|Top of the former Parmelia Formation - now formalised to Charlotte Sandstone of the Parmelia Group.  Geological Province:  Vlaming Sub-basin.||||||
24836|Charteris Basalt""|41252|6|Mentioned|p52|||See also Table 1||||||
78325|Charteris Formation|65008|6|Mentioned|p5|||Misspelt, see Charteris Basalt. Redefined by Bagas et al. (2004a) as included in the Kelly Subgroup.||Of the Kelly Subgroup||||
39736|Chearra Monzogranite|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 3020Ma.||||||07-NOV-08
39608|Cheeara Monzogranite|24534|5|Briefly described|Map legend|Archean|Archean| Of Yule Granitoid Complex.  Gneissic monzogranite to granodiorite.  Age: 2935Ma.||||||07-NOV-08
73845|Cheearra Granite|24550|6|Mentioned|p157|||Sinistral shear bands and sinistrally rotated K-feldspar clasts occur within this granite. Within the Pilbara Well Greenstone Belt. Geological Province: Pilbara Craton. See also p158 Fig. 7.12a.||||||07-FEB-11
29777|Cheela Spring Basalt|43037|5|Briefly described|Fig.2, p24|||Misspelling of Cheela Springs Basalt||||||
29777|Cheela Spring Basalt|73538|6|Mentioned|p2 Fig. 1B, p4|Orosirian|Rhyacian|Ages of 2209 +/- 10 Ma, 2030 +/- 6 Ma were reported by M�ller et al. (2005) and Martin et al. (1998).|2209 +/- 10 Ma, 2030 +/- 6 Ma|Wyloo Group, Lower||Underlain by Beasley River Quartzite. Overlain by Wooly Dolomite.|Mafic volcanics.|
38601|Cheratta Granitoid Complex|23783|5|Briefly described|p37 Tb. 3|Archean|Archean|||||||07-NOV-08
38601|Cheratta Granitoid Complex|23789|4|Described|p11|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38601|Cheratta Granitoid Complex|24550|5|Briefly described|p40, p137|Archean|Archean|Intruded by the Munni Munni Complex. Age: 3114+/-5Ma to 2994+/-2Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
77444|Cherrabun Formation|60386|5|Briefly described|p297|Lopingian|Guadalupian|Roebuck/Canning Basin. Limestone nearshore-shelf.||Of Liveringa Group.||||
77524|Cherrata Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
39980|Cherrata Granitoid Complex|24184|4|Described|p712, 710|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3130Ma (Nelson 1998) - oldest components 3150-3060Ma.||||||07-NOV-08
39728|Cherratta Granite|24192|6|Mentioned|p863 Tb.3, p864|Archean|Archean|Geological Province: Pilbara Craton. Not intended as a formal name but as a distinct geochemical unit within the Cherratta Granitoid Complex||||||07-NOV-08
73592|Cherratta Granitic Complex|63441|6|Mentioned|p35,36,37|Archean|Archean|Includes Railway, Elizabeth Hill and Maitland River Supersuites within its structure.||||||07-FEB-11
73592|Cherratta Granitic Complex|67201|4|Described|p11, p13, p15, p19, p23, p26-27, p44|||South of the Sholl Shear Zone. Maitland River Supersuite makes up much of this complex in the far west Pilbara.|||Tarlwa Pool Tonalite, Cliff Pool Tonalite, Maitland River Supersuite|Is intruded by Railway Supersuite. Whundo Group is thrust onto Cheratta Granitic Complex across Maitland Shear Zone.||
73592|Cherratta Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
31688|Cherratta Granitoid Complex|22449|6|Mentioned|P28, Table3 P27||Archean|Age of unit is 3115 Ma||||||07-NOV-08
31688|Cherratta Granitoid Complex|23484|4|Described|p17|Archean|Archean|Age: ~2990Ma. Geological Province: Pilbara Craton||||||07-NOV-08
31688|Cherratta Granitoid Complex|23780|5|Briefly described|p167|Archean|Archean|Of the Fortescue Group. Overlying Unit: Hardey Formation (unconformable)||||||07-NOV-08
31688|Cherratta Granitoid Complex|23784|5|Briefly described|p10|Archean|Archean|||||||07-NOV-08
31688|Cherratta Granitoid Complex|23793|5|Briefly described|p15|Archean|Archean|Age: c.3130 Ma||||||07-NOV-08
31688|Cherratta Granitoid Complex|23936|6|Mentioned|p3|||Geological Province: Pilbara Craton.||||||
31688|Cherratta Granitoid Complex|24023|5|Briefly described|p20|Archean|Archean|||||||07-NOV-08
31688|Cherratta Granitoid Complex|24192|5|Briefly described|p853|Archean|Archean|Geological Province: Pilbara Craton. Age: 3150-2944 Ma (Hoatson et al, 1992). Leucocratic granites||||||07-NOV-08
31688|Cherratta Granitoid Complex|24352|5|Briefly described|Map legend|Archean|Archean|Syenogranite to tonalite; locally porphyritic and generally foliated.   Age: ~2994Ma.   Geological Province: Pilbara Craton||||||07-NOV-08
31688|Cherratta Granitoid Complex|24353|4|Described|p1, 18|Archean|Archean|Overlying Unit: Fortescue Group (unconformable). Age: 3236-2940Ma. Geological Province: Pilbara Craton||||||07-NOV-08
31688|Cherratta Granitoid Complex|24541|3|Fully described|p1, p12, p30-32|Archean|Archean|Geological Province: West Pilbara Granite-Greenstone Terrane.  Age: oldest components 3236 - 3060 Ma. Unconformably overlain by the Fortescue Group to the southwest.||||||07-NOV-08
31688|Cherratta Granitoid Complex|24543|5|Briefly described|Map legend|Archean|Archean|Age: 3240-2940Ma.||||||07-NOV-08
31688|Cherratta Granitoid Complex|43822|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
31688|Cherratta Granitoid Complex|50300|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.  Age: c.3000Ma.||||||07-NOV-08
31688|Cherratta Granitoid Complex|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton. Age: 3240-2940 Ma||||||07-NOV-08
31688|Cherratta Granitoid Complex|50430|5|Briefly described|p164||Archean|3160-3060 Ma. In West Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
31688|Cherratta Granitoid Complex|61267|5|Briefly described|p71|Archean|Archean|Age: c. 3115-2925 Ma. Geological Provnce: Pilbara Craton.||||||07-NOV-08
31688|Cherratta Granitoid Complex|63372|4|Described|Map Legend|Archean|Archean|Age: 3000Ma. Geological Province: West Pilbara Granite-Greenstone Terrane. Syenogranite to granodiorite, locally biotite rich, foliated; metamorphosed.||||||07-NOV-08
31688|Cherratta Granitoid Complex|69299|3|Fully described|p1,p5 Fig.4,p8 Fig.5,p9-13,p15,p20,map|Archean|Archean|Of Mesoarchaean West Pilbara Granite-Greenstone Terrane, Pilbara Craton. Specific U-Pb SHRIMP ages on p10 Tb.3. Dated saples from near Waloo Waloo Pool and Mardeburra Pool discussed. Small inliers in north-west COOYA POOYA are syenogranite and monzogranite. SHRIMP U-Pb zircon ages on p12. Late components include c. 2950-2935 Ma intrusions.|c.3240-2930Ma; 2988+/-7Ma, 3006+/-6Ma SHRIMP U-Pb|||Contact with Whundo Group is partly tectonic (faulted) and partly intrusive; is unconformably overlain by Hardey Formation.|Syenogranite to tonalite; locally porphyritic and typically foliated; gneissic granitoid contains mafic xenoliths; metamorphosed.|
41223|Cheyne Spring Formation|50226|5|Briefly described|p428|||Of the Edmund Group.  Has mineralised horizons.||||||24-JUN-04
41303|Chiall Formation, lower|50188|6|Mentioned|p3|||Informal - see Chiall Formation.||||||16-JUL-08
74043|Chimingadgi Trondjhemite|60429|4|Described|p6 Fig. 3, p15|||Misspelt - should be Trondhjemite. Of Mount Edgar Granitoid Complex, eastern margin.Unconformably overlain by basal Fortsecue Gp.Intrudes Euro Basalt + Munganbrina Monzogranite. Geol.prov: Pilbara Craton. Whitish-grey, massive, medium-grained trondhjemite||||||07-FEB-11
74043|Chimingadgi Trondjhemite|65726|5|Briefly described|Map legend|Archean|Archean|[Mis-spelling of Trondhjemite] East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Grey-white, massive, even-grained biotite trondhjemite; hybrid amphibole-rich granitoid rock with mafic and ultramafic xenoliths.|
34339|Chimney Rock Oolite""|22718|6|Mentioned|P9|||||||||
39999|Chinaman Creek Chert Member|24184|6|Mentioned|p700|Archean|Archean|Parent: Talga Talga Subgroup. Geological Province: Pilbara Craton. Formerly considered part of the Duffer Formation||||||07-NOV-08
70217|Chinaman Creek chert|61579|5|Briefly described|p71|||Yielded abundant "microfossils"  called Apex "microfossils" (and attributed to Apex chert) - now known to have been collected at the "Microfossil" site at Chinaman Creek).||||||
38536|Chiratta Granitoid Compex|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38537|Chiratta Granitoid Complex|23813|5|Briefly described|p99|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38537|Chiratta Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p147 Tb.2-21|||West Pilbara. Poorly exposed.|||||Foliated monzogranite, granodiorite, migmatite; some porphyritic phases.|
23485|Chirup Formation|7433|6|Mentioned|p25 Fig.2, p32 Fig.8, p39. |Late Permian|Late Permian|Wallal and Samphire Embayments, Canning Basin. Fine, lagoonal? clastics.||||||
23485|Chirup Formation|13255|6|Mentioned|p376|Triassic|Permian|Marine sediments. Mentioned only as 'the Chirup and Blina Shales'.||||||
23485|Chirup Formation|37368|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
23485|Chirup Formation|38878|6|Mentioned|Map legend|Tatarian|Tatarian|||||||
23485|Chirup Formation|41474|6|Mentioned|p66|||||||||
23485|Chirup Formation|43173|6|Mentioned|54|Triassic|Permian|||||||
23485|Chirup Formation|44143|4|Described|p.435 Table 4-19|Permian|Permian|Up to 38m thick; interbedded grey to black carbonaceous shale, and fine grained to conglomeratic sandstone; shallow marine. Unconformably overlies Grant Group. Type section between 499 to 537m in Chirup 1 (MANDORA: 19deg 51' S, 120deg 26' E).||||||
23485|Chirup Formation|45153|2|Defined|App.4-80|Late Permian|Late Permian|||||||
23485|Chirup Formation|45158|3|Fully described|p18|||||||||
23485|Chirup Formation|66949|5|Briefly described|p24, p59 Appx.3|Permian|Permian|Burns et al. (1981). Superseded here: assigned to undifferentiated Liveringa Group. Late Permian. Type section detailed; only known from Chirup 1 499¿537 m, and BMR 04A Mandora, ?587¿612 m;. About 40m thick; shallow marine deposits.||||Unconformably overlies Grant Group. Lateral equivalent to Liveringa Group.|Interbedded grey to black carbonaceous shale, and fine-grained to conglomeratic sandstone.|05-NOV-15
23485|Chirup Formation|67202|6|Mentioned|p44 Fig.2.10|||Canning Basin. An aquiclude.||||||
73560|Christine Point Formation|36483|5|Briefly described|p69|||See also Christine Point  formation. Informal reference to Christine Point Clay. Geological Province: Canning Basin.||||||07-AUG-07
27367|Christopher Beds|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|Adelaidean or Carpentarian||||||
27367|Christopher Beds|30533|4|Described|p19|||See also Table 4||||||
27367|Christopher Beds|44155|5|Briefly described|p249 Tb.3-9|||1300m thick. Appears as Christopher beds.|||||Shale, siltstone, conglomerate, sandstone, altered basaltic material.|
27368|Christophers Beds|30895|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian and/or Adelaidean||||||
80252|Chunderloo Granite|71311|6|Mentioned|p797|||||||||
83317|Churchill Sand|73213|5|Briefly described|955, 956-957 Figs.1-2, 959, 961-962|||See also p966 Fig.14, 967-968, 970. Landward-ingressing due to coastal winds. See also Church Hill Sand (the current formal name) on pages 958 Fig.3(a), 961 Fig.8.||||Overlies Mowanjum Sand.|Orange quartzose sand derived from the Mowanjum Sandstone. Contains reworked plumes and sheets of midden shells and stone artefacts washed down from upslope deposits.|
69731|Cistern Formation, upper|24140|6|Mentioned|p216|||Informal - see Cistern Formation.  Originally included by Fitton et al (1975) as part of Constantine Formation (Whim Creek Group).||||||
38615|Cistern arkose, Upper|23784|5|Briefly described|p22|||Informal name for upper part of the Cistern Formation.||||||
38611|Cistern arkose, upper|23784|6|Mentioned|p22|||Informal name - see Cistern Formation.||||||
38614|Cistern conglomerate, Lower|23784|5|Briefly described|p22|||Informal name for lower part of the Cistern Formation.||||||
38612|Cistern conglomerate, lower|23784|6|Mentioned|p22|||Informal name - see Cistern Formation.||||||
28455|Cistern formation|32189|3|Fully described|p197|||||||||
24845|Cistern rhyolite|32189|6|Mentioned|p197|||||||||
24845|Cistern rhyolite|39101|6|Mentioned|Fig.20|||||||||
42466|Clanmyer Formation|12733|6|Mentioned|p565.|||Name replaced by Clanmeyer Formation which, in turn, became Clanmeyer Siltstone. Canning Basin. Contains oil-prone basal marine shales.||||||
42466|Clanmyer Formation|60702|5|Briefly described|p4|Famennian|Famennian|Thick marine shales - provide an oil reservoir seal.  Max. thickness: 400m.  Geological Province: Canning Basin.||||||
40765|Clarke Well Monzogranite|24494|5|Briefly described|p12|Archean|Archean|Age: 2640 +/- 8 Ma (Nelson, 1995). Intruded the Ida Fault.||||||07-NOV-08
40765|Clarke Well Monzogranite|64633|5|Briefly described|p16.|Neoarchean|Neoarchean|Stitches the Ida Fault in the Leonora-Laverton area.|2640 +/- 8 Ma (Nelson 1997).|||||
79811|Claudius Formation|69586|5|Briefly described|p11, p13|||Hosts the Redeemer gold deposit, dated at c.2638 Ma (Blewett and Czarnota, 2007), and the Waroonga (Emu) deposit. Locally known as the Mine Conglomerate.|||||Auriferous mafic and ultramafic conglomerates, strongly foliated and locally sheared, and finer-grained facies. Contains centimetre-scale clasts of granite and mafic rock in a mafic groundmass.|
35909|Clearville Formation|23348|5|Briefly described|218|Archean|Archean|||||||07-NOV-08
35909|Clearville Formation|66217|6|Mentioned|p5.|||Mis-spelling of Cleaverville Formation.||||||
33921|Cleaverville Greenstones|22471|4|Described|26-27|||Geological province: Pilbara Block.||||||23-JAN-08
39910|Cleaverville Group|24095|5|Briefly described|p45|Archean|Archean|Age: ~3.2Ga.  Geological Province: Pilbara Block.||||||07-NOV-08
39910|Cleaverville Group|24391|5|Briefly described|p8-3|Archean|Archean|Preserves three cycles of basaltic volcanism, felsic volcanism and chemical sedimentary deposition. Geological Province: Pilbara Block.||||||07-NOV-08
39910|Cleaverville Group|68574|6|Mentioned|p4|||Kiyokawa and Taira (1998), for the volcano-sedimentary succession comprising Regal and Cleaverville Formations. They renamed the latter unit as Snapper Beach Formation, which is informal (there being no official Snapper Beach in the area) and thus the original name is retained and the Cleaverville Group name is abandoned.||||||
80350|Cleaverville Supersequence|70775|6|Mentioned|p47|||Of Krapez 1993, and others [The author states that this supersequence is obsolete.].||||||05-FEB-18
24848|Cleaverville formation|42231|6|Mentioned|p336|||||||||
80349|Cleaverville group|70775|5|Briefly described|p47|||An informal [and obsolete] term first used by Kiyokawa (1993) to describe the combined Cleaverville and Regal Formations. Kiyokawa also created three new informal formations to make up this group; note however, that his proposals were not accepted by GSWA due to incompatibility with a range of geological and geochronological data.||||||05-FEB-18
34219|Cleia Shale|13292|6|Mentioned|pp309-310.|Jurassic|Jurassic|Sahul Syncline. Probable hydrocarbon source rock.||||||20-SEP-14
34219|Cleia Shale|22663|5|Briefly described|W97 -1-7Fig.4|Late Jurassic|Middle Jurassic|||||||
38130|Clianthus formation|23523|6|Mentioned|p994|||Informal - see Clianthus Formation. Of Grant Group.||||||
75825|Cliffs Ultramafic Unit|66192|5|Briefly described|p544, p545 Fig.2, p547, 550-552|||In Agnew-Wiluna Greenstone Belt. Ni-mineralisation: basal massive Ni-sulfide bodies overlain by horizons of disseminated, blebby and matrix sulfide. Extruded lava in a subaqueous environment; up to 420m thick.||||||09-MAR-12
75825|Cliffs Ultramafic Unit|70275|6|Mentioned|p471, 480|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||Is enclosed by Centenary Bore Basalt.||
75825|Cliffs Ultramafic Unit|70276|5|Briefly described|p783-787, 789-791|||Presented as [very informal] Cliffs ultramafic unit. Mount Keith Domain, Agnew-Wiluna greenstone belt, Yilgarn Craton. Mineralised. Proximal extrusive facies with variable thickness; over 150m thick locally. The basal flow unit hosts basal massive Ni-sulfide mineralisation (e.g. the giant MKD5 Ni deposit). S isotope data tabulated.||||Overlies Centenary Bore Basalt.|Comprises a sequence of differentiated olivine cumulates and spinifex-textured flow units. Generally vesicular.|
42401|Coal Measures Member""|23816|5|Briefly described|p240|||Superseded by the Cattamarra Coal Measures Member (Playford and Low, 1972). Geological Province: Perth Basin. Of the Cockleshell Gully Formation.||||||
24852|Coastal Limestone""|29382|6|Mentioned|p83|||Hydraulic conductivity.||||||
24852|Coastal Limestone""|30968|6|Mentioned|p30|||Considered excellent aquifer||||||
24852|Coastal Limestone""|31561|6|Mentioned|p10|||||||||
24852|Coastal Limestone""|31562|4|Described|p14|Pleistocene|Recent|Pleistocene - Recent. See also p10.||||||06-AUG-07
24852|Coastal Limestone""|31910|6|Mentioned|p24|||||||||
24852|Coastal Limestone""|32748|4|Described|p23|||Gage Roads No.2||||||
24852|Coastal Limestone""|32750|4|Described|p308|||||||||
24852|Coastal Limestone""|35282|6|Mentioned|p31|||||||||
24852|Coastal Limestone""|36293|6|Mentioned|p210|||||||||
24852|Coastal Limestone""|36405|6|Mentioned|p401|||||||||
24852|Coastal Limestone""|36705|6|Mentioned|p611|||||||||
24852|Coastal Limestone""|38071|5|Briefly described|p105|||||||||
24852|Coastal Limestone""|39554|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
24852|Coastal Limestone""|40359|6|Mentioned|p28|||||||||
24852|Coastal Limestone""|40367|6|Mentioned|p73|||Superseded by Tamala Laimestone.||||||07-AUG-07
24852|Coastal Limestone""|40400|6|Mentioned|p109|||Of Passmore (1970).   Now known as Tamala Limestone. Geological Province: Perth Basin.||||||06-AUG-07
24852|Coastal Limestone""|41341|6|Mentioned|p11|||||||||
24852|Coastal Limestone""|43297|6|Mentioned|p17|||Superseded by Tamala Limestone.||||||
24852|Coastal Limestone""|48610|14|Not recorded|p14|||Salt Marsh area.||||||
24852|Coastal Limestone""|48857|2|Defined|p.9-11|||||||||
24852|Coastal Limestone""|69558|6|Mentioned|p98|||Of Saint-Smith, 1912. Replaced by Tamala Limestone.||||||
32804|Cockatoo Series|45038|14|Not recorded|p.16||Late Devonian|Upper Devonian.||||||
25850|Cockleshell Gully Formation|12758|6|Mentioned|p16|Jurassic|Jurassic|Contained the informally named "Multicoloured Member" - now the Eneabba Formation. Thickness in type section: 589m.  Geological Province:  Northern Perth Basin.||||||
25850|Cockleshell Gully Formation|12759|6|Mentioned|p27, p32 Fig.15|Jurassic|Jurassic|Of Playford and Low (1972). Included Cattamarra Coal Measures Member, which was raised to Formation status by Mory (1994) and replaced Cockleshell Gully Formation in the Perth Region.||||||
25850|Cockleshell Gully Formation|22769|6|Mentioned|p755||Jurassic|Fluvial deposits.  Geological Province: Perth Basin.||||||17-JAN-06
25850|Cockleshell Gully Formation|23279|6|Mentioned|p23|||||||||
25850|Cockleshell Gully Formation|23816|4|Described|p240|Jurassic|Jurassic|Underlying unit: Lesueur Sandstone (conformable). Overlying unit: Cadda Formation (conformable). Max thickness: 2075 m. Contains the Eneabba Member and the Cattamarra Coal Measures Member.||||||
25850|Cockleshell Gully Formation|24058|4|Described|p112|Early Jurassic|Early Jurassic|Geological Basin: Perth Basin.||||||
25850|Cockleshell Gully Formation|24160|5|Briefly described|p94|||Perth Basin.|||Enneabba and Cattamarra Members.||Fine- to coarse-grained sandstone, with interbedded claystone and siltstone.|
25850|Cockleshell Gully Formation|24351|5|Briefly described|p38|Early Jurassic|Early Jurassic|Geological Province: Houtman Sub-basin. Includes non-marine sandstone and marginal marine sandstones.  May provide local seal (for oil).||||||13-DEC-07
25850|Cockleshell Gully Formation|29382|6|Mentioned|Table 10|||||||||
25850|Cockleshell Gully Formation|29689|4|Described|p105|||||||||
25850|Cockleshell Gully Formation|29693|6|Mentioned|Fig.7|||||||||
25850|Cockleshell Gully Formation|29721|6|Mentioned|p226|||||||||
25850|Cockleshell Gully Formation|29790|6|Mentioned|p92|||||||||
25850|Cockleshell Gully Formation|30217|6|Mentioned|p20|||See also P24 for hydrogeology||||||
25850|Cockleshell Gully Formation|30565|6|Mentioned|Fig.10|||||||||
25850|Cockleshell Gully Formation|30624|6|Mentioned|p1853|||||||||
25850|Cockleshell Gully Formation|30948|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25850|Cockleshell Gully Formation|30963|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
25850|Cockleshell Gully Formation|31237|6|Mentioned|p21|||||||||
25850|Cockleshell Gully Formation|31238|4|Described|p28|||||||||
25850|Cockleshell Gully Formation|31561|5|Briefly described|p26|||Early Jurassic||||||
25850|Cockleshell Gully Formation|31562|6|Mentioned|Fig. 3|||||||||
25850|Cockleshell Gully Formation|31568|5|Briefly described|p18|||L. Jurassic||||||
25850|Cockleshell Gully Formation|31859|6|Mentioned|p1063|||||||||
25850|Cockleshell Gully Formation|31896|6|Mentioned|p33|||L.Jurassic||||||
25850|Cockleshell Gully Formation|31899|6|Mentioned|p36|||||||||
25850|Cockleshell Gully Formation|31910|3|Fully described|p20|||Table 1||||||
25850|Cockleshell Gully Formation|32641|6|Mentioned|p5|||L.Jur.||||||
25850|Cockleshell Gully Formation|32642|6|Mentioned|p74|||Oil production||||||
25850|Cockleshell Gully Formation|32648|6|Mentioned|p32|||Liassic||||||
25850|Cockleshell Gully Formation|32649|6|Mentioned|p24|||||||||
25850|Cockleshell Gully Formation|32714|6|Mentioned|p83|||See also Fig.2||||||
25850|Cockleshell Gully Formation|32715|6|Mentioned|p1186|||Re oil||||||
25850|Cockleshell Gully Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
25850|Cockleshell Gully Formation|33166|6|Mentioned|p66|||Stratigraphy||||||
25850|Cockleshell Gully Formation|33386|6|Mentioned|Fig.7|||||||||
25850|Cockleshell Gully Formation|34134|6|Mentioned|p482|||Lower Jurassic||||||
25850|Cockleshell Gully Formation|34841|6|Mentioned|Fig.2|||||||||
25850|Cockleshell Gully Formation|35282|6|Mentioned|Fig.2|||See also Fig.6.||||||
25850|Cockleshell Gully Formation|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
25850|Cockleshell Gully Formation|35653|6|Mentioned|p1094|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
25850|Cockleshell Gully Formation|35968|5|Briefly described|p63|||Hydrogeology P65.||||||
25850|Cockleshell Gully Formation|35970|5|Briefly described|p83|||Discussion re hydrogeology.||||||
25850|Cockleshell Gully Formation|35983|6|Mentioned|Table 26|||||||||
25850|Cockleshell Gully Formation|36257|6|Mentioned|Table 2.1|||||||||
25850|Cockleshell Gully Formation|36265|5|Briefly described|Fig.3.26|Early Jurassic|Early Jurassic|Contains the Eneabba Member and Cattamarra Coal Measures Member. Geological province: Perth Basin.||||||04-MAR-08
25850|Cockleshell Gully Formation|36266|5|Briefly described|p150|||Geological Province: Perth Basin.||||||31-MAR-08
25850|Cockleshell Gully Formation|36293|2|Defined|p135|Jurassic|Jurassic|||||||
25850|Cockleshell Gully Formation|36890|3|Fully described|p240|||Formerly Cockleshell Gully Sandstone||||||
25850|Cockleshell Gully Formation|36911|6|Mentioned|p58|||||||||
25850|Cockleshell Gully Formation|37104|6|Mentioned|Fig.3|||||||||
25850|Cockleshell Gully Formation|37286|6|Mentioned|Figure|||||||||
25850|Cockleshell Gully Formation|37308|5|Briefly described|Table 4|||Hydrogeology P25.||||||
25850|Cockleshell Gully Formation|37309|4|Described|p15|||Groundwater P19.||||||
25850|Cockleshell Gully Formation|37340|6|Mentioned|p164|||||||||
25850|Cockleshell Gully Formation|37577|6|Mentioned|p64|||||||||
25850|Cockleshell Gully Formation|37688|6|Mentioned|p20|||||||||
25850|Cockleshell Gully Formation|38221|6|Mentioned|Fig.4|||Perth Basin||||||
25850|Cockleshell Gully Formation|38479|4|Described|p14|||||||||
25850|Cockleshell Gully Formation|38484|6|Mentioned|p7|||||||||
25850|Cockleshell Gully Formation|38486|6|Mentioned|p6|||||||||
25850|Cockleshell Gully Formation|38655|6|Mentioned|p6|||||||||
25850|Cockleshell Gully Formation|38732|6|Mentioned|p34|||||||||
25850|Cockleshell Gully Formation|38777|4|Described|p29|||||||||
25850|Cockleshell Gully Formation|39155|5|Briefly described|p17|||Aquifer characteristics||||||
25850|Cockleshell Gully Formation|39156|4|Described|p21|||||||||
25850|Cockleshell Gully Formation|39554|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
25850|Cockleshell Gully Formation|39854|6|Mentioned|p21|||||||||
25850|Cockleshell Gully Formation|39915|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
25850|Cockleshell Gully Formation|40304|4|Described|p37|||||||||
25850|Cockleshell Gully Formation|40305|4|Described|p79|||||||||
25850|Cockleshell Gully Formation|40358|6|Mentioned|p22|||||||||
25850|Cockleshell Gully Formation|40359|5|Briefly described|p22|||||||||
25850|Cockleshell Gully Formation|40794|5|Briefly described|p96|||||||||
25850|Cockleshell Gully Formation|40992|6|Mentioned|p6|||||||||
25850|Cockleshell Gully Formation|41172|5|Briefly described|p126|||||||||
25850|Cockleshell Gully Formation|41195|6|Mentioned|Fig.2|||||||||
25850|Cockleshell Gully Formation|41284|5|Briefly described|p90|||||||||
25850|Cockleshell Gully Formation|41454|6|Mentioned|p59|||||||||
25850|Cockleshell Gully Formation|41455|6|Mentioned|p67|||||||||
25850|Cockleshell Gully Formation|41589|6|Mentioned|p118|||||||||
25850|Cockleshell Gully Formation|41728|6|Mentioned|p441|||||||||
25850|Cockleshell Gully Formation|41729|5|Briefly described|p454|||||||||
25850|Cockleshell Gully Formation|41751|6|Mentioned|p6|||||||||
25850|Cockleshell Gully Formation|41781|4|Described|p10|||||||||
25850|Cockleshell Gully Formation|41782|5|Briefly described|p23|||||||||
25850|Cockleshell Gully Formation|41985|4|Described|p63|||See also P66||||||
25850|Cockleshell Gully Formation|41986|6|Mentioned|p34|||||||||
25850|Cockleshell Gully Formation|41989|4|Described|p109|||||||||
25850|Cockleshell Gully Formation|42075|5|Briefly described|Fig.7 P247|||||||||
25850|Cockleshell Gully Formation|42194|6|Mentioned|p31|||||||||
25850|Cockleshell Gully Formation|42434|4|Described|p5|||||||||
25850|Cockleshell Gully Formation|42734|5|Briefly described|map legend|Jurassic||||||||
25850|Cockleshell Gully Formation|43031|4|Described|p16,Fig.2.|||||||||
25850|Cockleshell Gully Formation|43062|5|Briefly described|p19,Table 2,p18|||||||||
25850|Cockleshell Gully Formation|43096|4|Described|p5|||see also Fig.2||||||
25850|Cockleshell Gully Formation|43212|5|Briefly described|p6||Jurassic|||||||
25850|Cockleshell Gully Formation|43297|6|Mentioned|p10,Fig.5 p9.|||'Cockleshell Gully Formation'is here abandoned.||||||
25850|Cockleshell Gully Formation|43347|6|Mentioned|5|||abandoned Mory, 1994||||||
25850|Cockleshell Gully Formation|43495|5|Briefly described|11|||||||||
25850|Cockleshell Gully Formation|44144|4|Described|p505 Tb.4-21, p509 fig 4-145, p514-515|Aalenian|Late Triassic|Type Section: Cockleshell Gully 30o07'45''S 115o11'23''E. 2km thick fluvial deposits. Reference Section: Eneabba 1; 1790-2978 m.|||Includes Eneabba and Cattamarra Members.|Conformably overlies Lesueur Sandstone. Is overlain conformably by Yarragadee and Cadda Formations. Correlates with Chapman Group.|Very fine- to very coarse-grained sandstone with interbedded siltstone, claystone and coal.|
25850|Cockleshell Gully Formation|44237|14|Not recorded|p.202,212|||||||||
25850|Cockleshell Gully Formation|44307|2|Defined|p11-15|||Formerly "Lesueur Sandstone". O/lain by Cadda Fm.& u/lain by Lesueur Sandstone. Believed to be basin equiv. of upper part of Chapman Group of Geraldton area.||||||
25850|Cockleshell Gully Formation|45168|6|Mentioned|p6|||||||||
25850|Cockleshell Gully Formation|48614|4|Described|p4,5,24,33,46|Early Jurassic|Late Triassic|See also other pages & Plates incl. App. 1 p12. Contains Cattamara Coal Member. H50-5,9.||||||
25850|Cockleshell Gully Formation|48615|6|Mentioned|P.21. Fig.2,6.|||(H50-6).||||||
25850|Cockleshell Gully Formation|48857|14|Not recorded|p.10|||Formerly Cockleshell Gully Sandstone.||||||
25850|Cockleshell Gully Formation|60726|5|Briefly described|p2-3, p5, throughout text. |Jurassic|Jurassic|Perth Basin. The caption on p2 erroneously dates this as Lower Cretaceous. |||Cattamarra Coal Measures Member.|||
25850|Cockleshell Gully Formation|61546|6|Mentioned|p385 Fig.5.|Early Jurassic|Early Triassic|||||||
25850|Cockleshell Gully Formation|67925|5|Briefly described|Ch2 p44-P45, Ch4 p8 fig 2|Jurassic|Permian|Misspelled as the Cocklesshell Gully Formation in Ch2 p44-p45. See also Ch5 p26, Ch8 p11.||||Overlies the Lesueur Sandstone. Overlain by the Cadda Formation and the Yarragadee Formation.||
25850|Cockleshell Gully Formation|68135|5|Briefly described|p52 fig 2b, p64|Aalenian|Hettangian|Perth Basin.|||Includes Cattamarra Coal Measures Member, Eneabba Member|Overlain by Cadda Formation|Silty sandstone, interbedded coal, mudstone and sandstone.|14-SEP-17
25850|Cockleshell Gully Formation|68811|5|Briefly described|p97, p98 fig 56, p155 app 1, p183 tbl 41|Jurassic|Jurassic|Hosts an aquifer in the Bunbury area. ||||Overlain by the' Superficial Formations' and the Yarragadee Formation. Unconformably overlain by the Leederville Formation.|Sand and shale.|16-APR-20
25850|Cockleshell Gully Formation|69182|6|Mentioned|Ch2 p46, Ch2 p99, Ch2 p101|||||||||
25850|Cockleshell Gully Formation|70128|6|Mentioned|p451|||Subsequently the Cattamarra Coal Measures.||||||
25850|Cockleshell Gully Formation|71780|14|Not recorded|p51 Table 1, p52, Plate 2||Early Jurassic|No white card.||||||
32577|Cody Formation|13615|6|Mentioned|p17|||Of Gorter and Davies (1999). Replaced herein by Cody Limestone.||||||
32577|Cody Formation|71623|2|Defined|p343-348, p362 App 1, p357, 359, 358|Roadian|Roadian|Carnarvon Basin. New name. Part of Pearce Cycle. Type section in Cody 1 between 3000 and 3,088 m. Identificed in 10 wells (listed). Thickness range >30m - >257m. Age: Ufimian.||Of Kennedy Group.||Overlain unconformably by Chinty Formation. Correlated with Beekeeper Formation, Pearce Formation.|Pale olive grey, bioclastic calcilutites.|
74637|Collie Burn Formation|42711|5|Briefly described|p17 Tb. 1|Permian|Permian|Of Fairbridge (1952). Previously called Middle or Collie Burn Phase/Horizon. Replaced by Collieburn Member in Cardiff Sub-basin and Premier Member in Muja Sub-basin, by Playford et al (1975), then Premier Coal Measures of the Collie Group.||||||11-AUG-08
24860|Collie-Burn Member|40359|6|Mentioned|Fig.3b|||||||||
40814|Collier 'Subgroup'|50188|6|Mentioned|p12|||Informal name. Upgraded to Collier Group.||||||14-JUL-04
40743|Collier Group, upper|24183|6|Mentioned|p6|||||||||
23495|Collier Subgroup|22589|6|Mentioned|p125||Proterozoic|||||||
23495|Collier Subgroup|22694|4|Described|p8|Proterozoic|Proterozoic|Bangemall Basin||||||
23495|Collier Subgroup|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
23495|Collier Subgroup|22905|6|Mentioned|p52-53|Mesoproterozoic|Mesoproterozoic|Superseded the Mucalana Subgroup of Muhling and Brakel (1985).  Now superseded by the Collier Group.||||||20-MAY-04
23495|Collier Subgroup|22907|6|Mentioned|41|||Parent Bangemall Group||||||
23495|Collier Subgroup|22940|4|Described|p20|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||17-JUL-08
23495|Collier Subgroup|23156|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|||||||
23495|Collier Subgroup|23403|6|Mentioned|p4|||||||||
23495|Collier Subgroup|23485|6|Mentioned|p30|||Superseded by Collier Group.||||||
23495|Collier Subgroup|23749|5|Briefly described|p14|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
23495|Collier Subgroup|24017|6|Mentioned|p5 Tb. 1|||Of the Bangemall Group.||||||07-AUG-08
23495|Collier Subgroup|24018|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
23495|Collier Subgroup|24115|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Geological Province: Collier Basin.||||||
23495|Collier Subgroup|24183|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Superseded by the Collier Group (Martin et al, 1999a). Of the Bangemall Group.||||||
23495|Collier Subgroup|24535|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Old name. Rocks now  incorprated into the Collier Group. Geological Province: Collier Basin.||||||26-NOV-13
23495|Collier Subgroup|40089|2|Defined|p43|Mesoproterozoic|Mesoproterozoic|||||||
23495|Collier Subgroup|40888|6|Mentioned|p153|||||||||
23495|Collier Subgroup|40938|6|Mentioned|Fig.3|||||||||
23495|Collier Subgroup|41768|6|Mentioned|p36|||||||||
23495|Collier Subgroup|42013|5|Briefly described|Map Legend|Proterozoic||||||||
23495|Collier Subgroup|42708|5|Briefly described|Plate 1|Proterozoic||||||||
23495|Collier Subgroup|43055|6|Mentioned|p20|||of Bangemall Group||||||
23495|Collier Subgroup|43209|5|Briefly described|map legend||Mesoproterozoic|of Bangemall Group.||||||
23495|Collier Subgroup|43492|6|Mentioned|9|||||||||
23495|Collier Subgroup|43561|6|Mentioned|p1439|||1450-1300 Ma||||||
23495|Collier Subgroup|43595|6|Mentioned|Fig 3-43,p348|||Age: 1.0-1.1 Ga||||||
23495|Collier Subgroup|43756|6|Mentioned|Fig.1,p534|||||||||
23495|Collier Subgroup|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23495|Collier Subgroup|44139|5|Briefly described|p277|||Of Bangemall Group. Considered by Williams et al (1976), Muhling & Brakel (1985) to include the Calyie Sandstone, which was subsequently included in Savory Group (Williams and Tyler, 1989).| | ||||05-MAR-18
23495|Collier Subgroup|44142|5|Briefly described|p309, p310 Tb.4-3, p311, p314 Tb.4-4|||See also p320-324, p329. Eastern Bangemall Basin. Eastern areas of this unit have been excised (Williams, 1990), with the Diebil Subgroup, from Bangemall Group and put in the new Savory Group (and thus Savory Basin). Younger than Edmund Subgroup. Correlated with Collier Subgroup.||Bangemall Group|Includes Backdoor and Ilgarari Formations, and Calyie and Wonyulgunna Sandstones.|Overlies Edmund Subgroup conformably in the W, unconformably in N and E. Unconformable on Troy Creek beds and Earaheedy Group (faulted against the latter). Unconformably underlies Savory Group.||13-MAR-18
23495|Collier Subgroup|50188|5|Briefly described|p2 Fig. 1, p15|||Of the Bangemall Group. Upper part was originally placed in the Savory Group which has since become mostly Sunbeam and Diasappointment Groups; and lower part tog. with Kahrban Subgroup were left in Bangemall Group, the latter now upgraded to supergroup.||||||16-JUL-08
23495|Collier Subgroup|50626|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Group.  Geological Province: Bangemall Basin.||||||
23495|Collier Subgroup|63869|6|Mentioned|p27, p39|||Superseded name; raised to Group status (Martin et al., 1999) following recognition of significant regional unconformity.||||||
23495|Collier Subgroup|64772|6|Mentioned|p13, p14 Fig.7, p20-21 Fig.10, p25|||Superseded Collier Group when Bangemall Basin stratigraphy was reviewed (Martin et al (1999).||||||25-NOV-13
23495|Collier Subgroup|65830|6|Mentioned|p8|||Elevated to Group rank by Martin et al. (1999) during revision of the former Bangemall Group.||||||
23495|Collier Subgroup|67183|5|Briefly described|p640, p644, p661, |Mesoproterozoic|Mesoproterozoic|Of the Bangemall Basin.|ca 1300-1100 Ma Martin et al. 1999|Bangemall Supergroup||Correlates with the Manganese Subgroup.|Sedimentary.|
23495|Collier Subgroup|67201|6|Mentioned|p53 Fig.40|||Shown as Collier-Managanese Subgroups. Bangemall Basin.||||||
40815|Collier Subgroup""|50188|6|Mentioned|p16|||See Collier Subgroup.||||||16-JUL-08
40816|Collier Subgroup, lower|50188|5|Briefly described|p15|||Informal name.  Of the Bangemall Group.||||||16-JUL-08
40817|Collier Subgroup, upper|50188|5|Briefly described|p15|||Informal name. Of the Bangemall Group.||||||16-JUL-08
41224|Collier group|50226|6|Mentioned|p427|||Informal - see Collier Group.||||||
34419|Collier subgroup|22716|6|Mentioned|table4, p237|Ectasian|Ectasian|Age: 1300 Ma. Part of the Bangemall Basin succession.||||||
37216|Colville sandstone|23989|5|Briefly described|p54 Fig. 46|Cenozoic|Cenozoic|Informal name. Geological Province: Yilgarn Craton||||||03-MAR-10
73602|Comet Vale granite|63463|6|Mentioned|p584 Fig. 1, p586|||In the Eastern Goldfields Province.||||||
78075|Como Sandstone|68254|6|Mentioned|p1036 Fig.2|Cretaceous|Cretaceous|Presented as Como Sandstone in figure. See Como Sandstone Member in this paper. ||||||
35924|Comstock "Andesite"|23348|6|Mentioned|225|||||||||
28466|Comstock andesite|32189|5|Briefly described|p197|||||||||
28466|Comstock andesite|39101|6|Mentioned|Fig.20|||||||||
41081|Condenser dolerite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain.  Age: 2676 +/- 4Ma (zircon).  Of the Black Flag Beds.||||||07-NOV-08
80936|Condensor Dolerite|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. Age from granophyre, U-Pb zircon SHRIMP (Carey, 1994).|2680+\-8 Ma (Carey, 1994)|||Intrudes into lower Black Flag Group. Correlable to Golden Mile Dolerite.||
80936|Condensor Dolerite|72049|5|Briefly described|p253, p257-p259, p267-p268|||St Ives. This unit has magmatic affinities with dated but unnamed rocks in the present study. See also Condenser Dolerite p258, 272.|2680 +/- 8 Ma (Carey, 1994)|||||18-MAR-19
80936|Condensor Dolerite|72057|4|Described|p238-240,242-243,246-247,249|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Contact with Black Flag Group host sediments is irregular, indicating emplacement into unconsolidated sediments and at relatively shallow depths. Interpreted as an intrusive sill, based on common coarse (>3mm) groundmass grain size, thin hosting sediments indicating relatively flat paleo-depositional enviroment (thus not conducive for lava ponding) and extensive sheet-like geometry. Likely connected to Junction Dolerite, because they are laterally extensive and occur on opposite limbs on an anticline, similar geochemistry and occur at the same stratigraphic level, and hosted within bedded mudstone, siltstone and sandstone of the Black Flag Group sediments. U-Pb SHRIMP age of 2680+\-8 Ma on zircons from the granophyre lithofacies(Carey, 1994). Drilled and studied in 5 locations on the St Ives property as part of this study. Thickness varies along strike: 76-225m, averaging 172m.||Unit of Black Flag Group.|||Aphyric basalt, grading upward through dolerite and gabbro into pyroxenite, and up into dolerite, minor gabbro and quartz gabbro.|
80936|Condensor Dolerite|72095|5|Briefly described|p10-12,15-17,20|||Kambalda Region, Eastern Goldfields, Yilgarn Craton. Compositionally indistinguishable from Low-Th Basalt (LTB) of Barnes et al., 2012. Detailed geochemistry is described.||||||
80936|Condensor Dolerite|72252|6|Mentioned|p11|||St. Ives Au-Ni camp, Kambalda Domain, Yilgarn Craton. 5 - 500m thick.|||||Intrusive tholeiitic differentiated dolerite and gabbro.|
80936|Condensor Dolerite|73596|6|Mentioned|p1161|Neoarchean|Neoarchean|Kalgoorlie area.|2680 +/- 8 Ma.|||Intrudes Black Flag Group. Correlated with Mount White Dolerite.||
69033|Condren Formation|44231|5|Briefly described|Map Legend|Permian|Permian|Of the Liveringa Group.  Undifferentiated section and three unnamed sections: sandstone and siltstone; medium-grained quartz sandstone; ferruginous siltstone and snadstone; medium-grained quartz sandstone, silty sandstone. All are fluvial.||||||
74119|Conndoondoo Gneiss|24197|6|Mentioned|p69|||Of Williams (1986) but possibly misspelt; place name is Coondoondoo. Informally referred to as the Conndoondoo Gneiss dome, parts of which are incorporated into the Minnie Creek Supersuite.||||||07-FEB-11
23502|Coocoowilya Formation|42533|3|Fully described|p81|||Name reserved.||||||
23502|Coocoowilya Formation|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p41-42|Archean|Archean|See also p44 Fig.2-46, p47. Of Murchison Province||Mount Farmer Group|||Basal 350m of fine- to medium-grained amphibolite; then 300m of pelitic/psammitic and siliceous aphanitic to feldspar-phyric schists with pods of foliated granitoid; at the top, amphibolite (500m thick) with abundant lenses of basaltic breccias.|
23502|Coocoowilya Formation|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Tholeiitic basalt, mafic pyroclastic rocks, felsic volcaniclastic rocks.|
23502|Coocoowilya Formation|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
79283|Coodardy Formation|67129|4|Described|p18 Fig.19, p36-38|Archean|Archean|Murchison Domain, Youanmi Terrane.|~2800 Ma|Basal Polelle Group.|||Quartzite and overlying banded iron-formation.|06-SEP-17
79283|Coodardy Formation|68698|5|Briefly described|p4-5|Neoarchean|Neoarchean|||Polelle Group.||Overlies Yaloginda Formation (Norie Group). Is overlain by Meekatharra Formation.|Thin quartzitic unit.|
79283|Coodardy Formation|69583|5|Briefly described|p47, p49|Neoarchean|Neoarchean|Murchison Domain. See also Coodardy Pool Formation (Plate 2).||Basal Polelle Group.|||Quartzite.|
79283|Coodardy Formation|69584|5|Briefly described|p5 Fig.2|Neoarchean|Neoarchean|||Polelle Group||Overlies the Yaloginda Formation, overlain by the Meekatharra Formation|Quartzite and banded-iron formation.|
79283|Coodardy Formation|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Polelle Group.||||
79283|Coodardy Formation|70020|4|Described|p117-118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Thickness: 100m.||Unit of Polelle Group.||Overlain by Meekatharra Formation. Underlain by Yalogina Formation/Norie Group.|Basal quartzite and BIF.|
79283|Coodardy Formation|70030|4|Described|p190,192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Polelle Group.|Includes Lordy Basalt.|Lowermost unit of Polelle Group. Conformably overlain by Meekatherra Formation. Underlain by Yaloginda Formation/Norie Group.|Quartzite and iron-formation.|17-JUL-19
79283|Coodardy Formation|71168|4|Described|p7-p8|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton. Up to 100m thick.|c. 2790 Ma|Polelle Group||Overlies the Yaloginda Formation. Overlain by the Meekatharra Formation.|Basal quartzite and banded-iron formation.|
39981|Cooeenia Basalts|24184|5|Briefly described|p702, p699 Fig.3|Archean|Archean|Parent: Gorge Creek Group. Overlying Unit: Cattle Well Formation. Geological Province: Pilbara Craton. Intruded by ultramafic and mafic sills of Dalton Suite||||||07-NOV-08
40060|Cooglegong granite|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.2.85 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
69016|Cooieena Basalt|50189|4|Described|p17, 27|Archean|Archean|Of the Gorge Creek Group. Massive and pillowed basalt, silicified basaltic andesite, minor high Mg basalt. Disconformably overlies: Cundaline Formation; unconformably overlies: Nimingarra Iron Formation; overlain unconformably by: Fortescue Group.||||||07-NOV-08
69016|Cooieena Basalt|60429|2|Defined|p17, p37 Appdx. 1|Archean|Archean|Unconformable on Cundaline Fm + Nimingarra Iron Fm;  unconformably below Fortescue Group + EelCk Fm in east. Age: <c.3244Ma. Max. thickness: ~1500m. Massive + pillowed tholeiitic basalt, hyaloclastic breccia, silicified basaltic andesite, metamorphosed.||||||07-FEB-11
73591|Cooke Creek Monzogranite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Misspelt - should be Cookes Creek Monzogranite. Supersedes Cookes Creek Granite. Geological province: Pilbara Craton.||||||07-FEB-11
73591|Cooke Creek Monzogranite|64653|5|Briefly described|Map Legend|Archaean|Archaean|Geological Province: Pilbara Craton. Monzogranite, fine to medium grained, biotite-bearing, seriate to feldspar porphyritic; intruded by quartz-barite veins; metamorphosed.||||||07-FEB-11
73591|Cooke Creek Monzogranite|65008|4|Described|p5, p13, p20, p21, p26, p28, p41|Mesoarchean|Mesoarchean|East Pilbara Granite-Greenstone Terrane. Intrusive age interpreted as ca. 2850 Ma.|ca. 2850|||Intrudes the Warrawoona Group.|Monzogranite, fine to medium grained, biotite-bearing, seriate to feldspar porphyritic; intruded by quartz-barite veins; metamorphosed.|
24866|Cookes Creek Granite|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
24866|Cookes Creek Granite|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
24866|Cookes Creek Granite|24193|5|Briefly described|p875 Fig.2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
24866|Cookes Creek Granite|30484|6|Mentioned|p56|||Re age dates||||||
24866|Cookes Creek Granite|31308|6|Mentioned|Table 12|||Geochronology||||||
24866|Cookes Creek Granite|35726|6|Mentioned|p60|||||||||
24866|Cookes Creek Granite|37460|6|Mentioned|p126|||||||||
24866|Cookes Creek Granite|38510|6|Mentioned|Table 1|||||||||
24866|Cookes Creek Granite|38514|5|Briefly described|Table II|||||||||
24866|Cookes Creek Granite|39697|3|Fully described|p50|||See also p23||||||06-APR-16
24866|Cookes Creek Granite|44150|5|Briefly described|p147 Tb.2-21|||40 sq. km.|2600 Ma (de Laeter et al., 1977).|||Intrudes Warrawoona Group.|Syenogranite, monzogranite, porphyritic varieties.|
24866|Cookes Creek Granite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Of Split Rock Supersuite. Superseded by Cookes Creek Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
37994|Cookilya Sandstone|23403|4|Described|p8|Late Permian|Early Permian|Of Kennedy Group.||||||
39745|Cool bro Sandstone|24194|6|Mentioned|p901 Tb.1|||Informal name - see Coolbro Sandstone. Geological Province: Paterson Orogeny||||||
81297|Coolamen hornblende-biotite granite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Jungar Suite.||||
81780|Coolbina Intrusion|69185|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||||||
77782|Coolbro Formation|67182|6|Mentioned|p678|Neoproterozoic|Neoproterozoic|See the correct name: Coolbro Sandstone. ||||||
24867|Coolbye Shale Member""|35976|6|Mentioned|Table 16|||||||||
78814|Cooleyna Group|64635|5|Briefly described|p4 Fig.3|Maastrichtian|Aptian|[Mis-spelling of Coolyena].|||Includes Osborne and Lancelin Formations; Molecap and Poison Hill Greensands; Gingin Chalk.|||
34476|Coolibah tuff member|22754|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Informal subdivision of Koongie Park Formation. Max. thickness: >100m.||||||07-NOV-08
32762|Coolkilya Formation""|45016|14|Not recorded|p.174|||Ref. to Teichert 1952,1957. Invalid as it includes an important disconformity.||||||
74727|Coolkiya Sandstone|64580|6|Mentioned|map legend|||Of Kennedy Group. Misspelling of Coolkilya Sandstone.||||||
74727|Coolkiya Sandstone|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||||||
29282|Coolyana Group|35638|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Misspelling of Coolyena? Lower - Upper Cretaceous.||||||
32594|Coolyia Conglomerate|45923|4|Described|p.69|||||||||
32593|Coolyia Creek Conglomerate|45923|4|Described|p.66,69||Quaternary|||||||
36959|Coolyia Creek Tonalite|23416|5|Briefly described|Map Legend|Archean|Archean|Of Shaw Granitoid Complex, Pilbara Craton||||||07-NOV-08
36959|Coolyia Creek Tonalite|23755|4|Described|p48|Archean|Archean|Of North Shaw Suite.||||||07-NOV-08
36959|Coolyia Creek Tonalite|24531|6|Mentioned|p27|||Of the North Shaw Suite (northern part of Shaw Granitoid Complex).||||||
36959|Coolyia Creek Tonalite|63441|5|Briefly described|p7 Tb. 2|Archean|Archean|Superseded by Coolyia Creek Granodiorite.||||||07-FEB-11
36959|Coolyia Creek Tonalite|69167|6|Mentioned|142962.1.pdf|Archaean|Archaean|Age derived from medium grained tonalite sample (142962.1.pdf)|3469 Ma +/- 2 Ma (SHRIMP)|North Shaw Suite||||
36959|Coolyia Creek Tonalite|71137|6|Mentioned|p3|Archean|Archean|Eastern Pilbara. Metamorphosed at 2907 +/- 7 Ma (40Ar/39Ar hornblende; Wijbrans and McDougall, 1987).||||||
38603|Coolyia Creek granodiorite|23783|5|Briefly described|p115 Fig. 64|Archean|Archean|Informal - see Coolyia Creek Granodiorite.||||||07-NOV-08
38603|Coolyia Creek granodiorite|50427|6|Mentioned|p188 Fig.9|Archean|Archean|Informal||||||07-NOV-08
79614|Coomb Bore Granite|64771|5|Briefly described|p25-26|Neoarchaean|Neoarchaean|A small (1x3 km), NW-trending pluton. Forms prominent bouldery hills. Proportion of K-feldspar increases to NW. Metamorphosed to at least amphibolite conditions, with weak to moderate foliation (biotite/quartz). Mineralogy and deformation briefly described. SHRIMP U-Pb zircon crystallisation ages from two granodiorite samples.|c.2690 Ma (Nelson, 2002, 2004).||||Monzogranite predominant with granodiorite and syenogranite phases. Typically medium-grained, equigranular to porphyritic, dark pinkish grey to pale red.|
72413|Coomberarie Formation, upper|48823|6|Mentioned|p21, p23|||Informal - see Coomberarie Formation.||||||
27133|Coomberdale Chert|24058|5|Briefly described|p110|Precambrian|Precambrian|Max. thickness: 1024m.  Geological Basin: Perth Basin.||||||
27133|Coomberdale Chert|24160|6|Mentioned|p26, p27 Tb. 14|Proterozoic|Proterozoic|||Coomberdale Subgroup||||
27133|Coomberdale Chert|24410|5|Briefly described|p142 Tb. 60|Proterozoic|Proterozoic|?Together with Dudawa Beds, superseded by Jingemia Dolomite of Coomberdale Subgroup (Moora Group). ||||||
27133|Coomberdale Chert|29548|6|Mentioned|p231|||||||||
27133|Coomberdale Chert|31051|6|Mentioned|p78|||||||||
27133|Coomberdale Chert|31154|6|Mentioned|p71|||||||||
27133|Coomberdale Chert|34203|6|Mentioned|p15|||?Proterozoic.||||||
27133|Coomberdale Chert|34705|5|Briefly described|p398|||||||||
27133|Coomberdale Chert|34737|6|Mentioned|p355|||||||||
27133|Coomberdale Chert|34999|6|Mentioned|p123|||||||||
27133|Coomberdale Chert|35282|6|Mentioned|p9|||||||||
27133|Coomberdale Chert|36293|2|Defined|p65|Proterozoic|Proterozoic|||||||
27133|Coomberdale Chert|36872|3|Fully described|p76|||||||||
27133|Coomberdale Chert|37460|6|Mentioned|p178|||||||||
27133|Coomberdale Chert|37577|6|Mentioned|p69|||See also P80.||||||
27133|Coomberdale Chert|38988|6|Mentioned|p13|||||||||
27133|Coomberdale Chert|40089|6|Mentioned|p148|||||||||
27133|Coomberdale Chert|40347|6|Mentioned|p16|||||||||
27133|Coomberdale Chert|40349|6|Mentioned|p14|||||||||
27133|Coomberdale Chert|41271|6|Mentioned|p228|||||||||
27133|Coomberdale Chert|43495|6|Mentioned|5|||||||||
27133|Coomberdale Chert|48848|14|Not recorded|p.23|||||||||
27133|Coomberdale Chert|61811|6|Mentioned|p36.|||Source of the large quartzitic glacial erratic known as 'White Horse' within the Nangetty Formation at 'Mungaterra' property.||||||
27133|Coomberdale Chert|64635|6|Mentioned|p18|||Near Moora. Source of the largest glacial erratic in Nangetty Formation, the quartzitic 'White Horse' on 'Mungaterra' homestead.||||||
27133|Coomberdale Chert|71781|4|Described|p55|||Unit in Moora Group.||||||
24872|Coondoon Conglomerate|30881|5|Briefly described|p527|||||||||
24872|Coondoon Conglomerate|34135|6|Mentioned|p15|||Middle Proterozoic.||||||
24872|Coondoon Conglomerate|36884|6|Mentioned|p156|||||||||
24872|Coondoon Conglomerate|39697|6|Mentioned|p14|||||||||
24872|Coondoon Conglomerate|40089|4|Described|p58|||||||||
24872|Coondoon Conglomerate|41669|6|Mentioned|p36|||||||||
24872|Coondoon Conglomerate|44297|14|Not recorded|p.5,7,10,17|||(F51-9).||||||
24872|Coondoon Conglomerate|44298|14|Not recorded|map legend||Proterozoic|||||||
29954|Coondoon Conglomerate""|43055|6|Mentioned|p21|||Superseded by Coondoon Formation||||||
39885|Cooneeina Basalt|23783|5|Briefly described|p17|||Of Gorge Creek Group.||||||
39885|Cooneeina Basalt|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group.  Pillowed and massive basalt, hyaloclastic breccia and silicified basaltic andesite.||||||07-NOV-08
40506|Cooneina Basalt|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
38082|Coongan Volcanics, Lower|23570|6|Mentioned|p232 Appendix 1|||Informal name - see Coongan Volcanics.||||||
38085|Coongan Volcanics, Upper|23570|6|Mentioned|p235 Appendix 1|||Informal - see Coongan Volcanics.||||||
70137|Coonieena Basalt Member|63441|2|Defined|p5 Tb.1, p29|Archean|Archean|Of Bookingarra Fm (Croydon Gp). Formerly Coonieena Basalt (Gorge Creek Gp) of Williams (1999) on MUCCAN. Disconformably overlies Cundaline Fm; disconformably overlain by Cattle Well Fm. Thickness: 1630m.Geological province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
70137|Coonieena Basalt Member|63538|4|Described|p10, p16, p35|Archean|Archean|Of Bookingarra Formation. Geological Province: Pilbara Craton. Massive, but locally include vesicular layers.||||||07-FEB-11
70137|Coonieena Basalt Member|64632|6|Mentioned|p203|||Basalt on northeastern margin of the East Pilbara terrrane. Compared to Loudens and Negri Volcanic Members, and Salt Well Member.|||||Basalt interbedded with clastic sedimentary rocks.|
70137|Coonieena Basalt Member|66217|6|Mentioned|p43.|||||Unit in Bookingarra Formation.||||
70137|Coonieena Basalt Member|67201|5|Briefly described|p21 Fig.12, p61|||Fig.12 after Van Kranendonk et al. (2006). See also Coonieena Basalt.||||||
70137|Coonieena Basalt Member|72668|6|Mentioned|p7-8, p15|||Shown as Coonieena Basalt p7 Fig 5 and also p15 (as well as full name) and p24. LREE basalts.||Bookingarra Formation.|||Basal conglomerate, basalt to komatiitic basalt.|13-JAN-22
40189|Coontarunah Group|24182|5|Briefly described|p93 Fig. 3|||Geological Province: Pilbara Craton.||||||
39884|Coonterunah Basalt|24550|6|Mentioned|p66|||Informal - see basalt units of Coonterunah Group (Double Bar and Table Top Formations).||||||07-FEB-11
40160|Coonterunah Gabbros|24621|6|Mentioned|p79 Fig. 6|||Informal reference to specific gabbro rocks within the Coonterunah Group.||||||
32209|Coonterunah Group|23206|5|Briefly described|Fig.1|||Age 3.51Ga.||||||
32209|Coonterunah Group|23416|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup, Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|23755|4|Described|p16|Archean|Archean|See also page 17 table 1.  Max. thickness: 6700 m.||||||07-NOV-08
32209|Coonterunah Group|23783|4|Described|p11|Archean|Archean|Intruded by Carlindi Granitoid Complex.  Maximum Thickness: 5900m.||||||07-NOV-08
32209|Coonterunah Group|23784|5|Briefly described|p2|Archean|Archean|Age: c.3515Ma.||||||07-NOV-08
32209|Coonterunah Group|23807|6|Mentioned|p109 Fig. 1|||Geological Province: Pilbara Craton.||||||
32209|Coonterunah Group|23891|5|Briefly described|p89|Archean|Archean|Of Mount Bruce Supsergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|23936|4|Described|p2|Archean|Archean|Age: ca. 3515 Ma. Geological Province: Pilbara Craton. Unconformably overlain by Warrawoona Group.||||||07-NOV-08
32209|Coonterunah Group|23956|4|Described|p1264|Archean|Archean|Age: ca. 3.52 Ga. Unconformably overlain by the Warrawoona Group. Geological Province: Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|24016|5|Briefly described|p293 (in title only)|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|24025|4|Described|p9 Tb. 1|Archean|Archean|Includes Double Bar, Coucal and Table Top Formations.  Age: c.3515Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Pilbara Supergroup.  Geological Province: Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|24166|4|Described|p9|Archean|Archean|Parent: Pilbara Supergroup.   Age: c.3515Ma.   Geological Province: Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|24184|4|Described|p699|Archean|Archean|Of the Pilbara Supergroup. Geological Province: Pilbara Craton. Age: ca.3.51-3.50Ga. Intruded by Carlindi Granitoid Complex||||||07-NOV-08
32209|Coonterunah Group|24186|4|Described|p776, 777 Fig.2|Archean|Archean|Age: ca. 3515Ma (Buick et al, 1955). Overlying Unit: Warrawoona Group. Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|24187|5|Briefly described|p776, 777 Fig.2|Archean|Archean|Age: ca. 3515 Ma (Buick et al, 1995). Unconformably underlies Warrawoona Group. Geological Province: Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|24327|5|Briefly described|Map Legend|Archean|Archean|Parent: Pilbara Supergroup.  Includes the Coucal and Table Top Formations.  Age: c.3515.  Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|24349|5|Briefly described|Map legend|Archean|Archean|Of Pilbara Supergroup.   Age: c.3515Ma. Geological Province: Pilbara Craton||||||07-NOV-08
32209|Coonterunah Group|24531|5|Briefly described|p5|Archean|Archean|Of the Pilbara Supergroup.  Unconformably underlies the Warrawoona Group.  Age: c.3515Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|24533|5|Briefly described|p4|Archean|Archean|Age: c.3515-3498Ma.||||||07-NOV-08
32209|Coonterunah Group|24550|5|Briefly described|p30, p31 Tb. 3.1|Archean|Archean|Unconformably overlain by Warrawoona Group. Age: ca 3515Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
32209|Coonterunah Group|24590|5|Briefly described|p28 Fig. 1.2|Archean|Archean|Includes: Table Top, Coucal and Double Bar Formations. Age: ca3515Ma. Geological Province: Pilbara Craton. See also p166.||||||07-FEB-11
32209|Coonterunah Group|24621|4|Described|p75|Archean|Archean|Unconformably overlain by Warrawoona Group.  Age: ~3.52Ga.  Max. thickness: 6km.  Tholeiitic basalt and gabbro with significant rhyolitic to andesitic volcanic and volcaniclastic deposits.  Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|50379|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|50423|4|Described|p216||Archean|3515 Ma. Dominantly basaltic. Unconformably overlain by lower Warrawoona Group. East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
32209|Coonterunah Group|50427|4|Described|p182 Fig.5|Archean|Archean|Age: 3520-3490 Ma. Overlain conformably by Talga Talga Subgroup and unconformably by Kelley Subgroup. Overlies younger granitoid rocks. Of Pilbara Supergroup.||||||07-NOV-08
32209|Coonterunah Group|50430|4|Described|p158 Tb.1||Archean|Deposited 3498-3515 Ma. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
32209|Coonterunah Group|50544|5|Briefly described|p18|Archean|Archean|Of the Pilbara Supergroup.  Age: ~3.5Ga.  Not on the YARRIE sheet.||||||07-NOV-08
32209|Coonterunah Group|60112|6|Mentioned|p107 Fig.1, p109 Fig.2, |||Mis-spelt as Coonterunnah in Fig.2.|||Includes Double Bar Formation.|||
32209|Coonterunah Group|60636|5|Briefly described|p29|Archean|Archean|Age: ~3.47-3.46Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
32209|Coonterunah Group|61111|5|Briefly described|p96 Fig.2||Paleoarchean||c.3515 Ma.|||||
32209|Coonterunah Group|61252|6|Mentioned|p66-67 Fig.2|||See also p68.||||||
32209|Coonterunah Group|61253|5|Briefly described|p51|Archean|Archean|Downgraded and redefined as the Coonterunah Subgroup of the Warrawoona Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|61257|5|Briefly described|p355 Tb. 1|Archean|Archean|Basalts with some cherty layers.  Geological Province: North Pole Dome of the Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|61266|4|Described|p55, p56, p58 Tb.1|Archean|Archean|Age: c. 3515 Ma (Buick et al., 1995). Unconformably underlies Warrawoona Group; overlain by Strelley Pool Chert across a paraconformity to an angular unconformity. Intruded by Carlindi Granitoid Complex. Max. thickness: ~6000m. Geol. Prov: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Unconformably overlain by Warrawoona Group. ||||||07-NOV-08
32209|Coonterunah Group|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Age: c.3515Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32209|Coonterunah Group|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Redefined as Coonterunah Subgroup (Warrawoona Group).||||||07-FEB-11
32209|Coonterunah Group|63649|5|Briefly described|p200|Archean|Archean|Of the Pilbara Supergroup. Age: ca.3.52Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
32209|Coonterunah Group|64328|5|Briefly described|p56 Tb. 1|||Includes Table Top and Coucal Formations.||||||07-FEB-11
32209|Coonterunah Group|65825|6|Mentioned|p5. |Archean|Archean|||Unit in Pilbara Supergroup according to Van Kranendonk et al. (2001, 2002).||||
32209|Coonterunah Group|66217|6|Mentioned|p8.  |||Rocks ascribed to this unit have been included in the Coonterunah Subgroup by Van Kranendonk et al. (2006a).||||||
32209|Coonterunah Group|71041|6|Mentioned|p44|Paleoarchean|Paleoarchean||3515 Ma|||||
40159|Coonterunah Magnesian Basalts|24621|6|Mentioned|p79 Fig. 6|||Informal reference to specific basalts within the Coonterunah Group.||||||
40161|Coonterunah Tholeiites|24621|6|Mentioned|p79 Fig. 6|||Informal reference to tholeiitic rocks within the Coonterunah Group.||||||
40164|Coonterunah basalts|24621|5|Briefly described|p81-82|||Informal reference to the basalts within the Coonterunah Group.||||||
40156|Coonterunah greenstones|24621|6|Mentioned|p73 Fig. 3|||Informal reference to part of the Coonterunah Group.||||||
73872|Coonterunah group|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Informal/misspelt - see Coonterunah Group. Age: 3515Ma. Includes Double Bar, Coucal and table Top Formations.||||||07-FEB-11
31376|Coonterunah succession|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3520-3400Ma||||||07-NOV-08
31376|Coonterunah succession|23255|6|Mentioned|p46 Fig.2||Archean|Rhyolite member dated at 3515+/-3Ma.||||||07-NOV-08
31376|Coonterunah succession|43562|4|Described|p575|||Age of rhyolite from middle of succession : 3515 +/- 2.7 Ma U-Pb SHRIMP. Succession intruded by Carlindi porphyritic microgranite (age: 3467.6 +/- 3 Ma).||||||30-APR-13
31376|Coonterunah succession|61266|6|Mentioned|p55|||Informal name. Upgraded to group status.||||||05-MAY-06
40155|Coonterunah-Warrawoona basalts|24621|5|Briefly described|p78|Archean|Archean|Informal compound term for the basalts of the Coonterunah and Warrawoona Groups.  Geological Province: Pilbara Craton.||||||07-NOV-08
40165|Coonterunah-Warrawoona tholeiitic basalts|24621|6|Mentioned|p82|||Informal compound term for the tholeiitic basalts of the Coonterunah and the Warrawoona Groups.||||||
38356|Coonterunnah Group|23813|5|Briefly described|p101|Archean|Archean|Bimodal mafic/felsic volcanics, minor komatiitic basalt.  Age: 3515Ma.  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
38356|Coonterunnah Group|23936|6|Mentioned|p28|||Misspelt - see Coonterunah Group.||||||
38356|Coonterunnah Group|24166|5|Briefly described|p3, p7|Archean|Archean|Misspelt - see Coonterunah Group.  Age: c.3515 (Buick et al, 1995; Van Kranendonk, 1998)||||||07-NOV-08
39722|Coonturunah Group|24185|5|Briefly described|p735 Fig.2, p737 Tb.2|Archean|Archean|Age: 3.50-3.52 Ga. Geological Province: Pilbara Craton||||||07-NOV-08
42475|Coor-de-Wandy formation|50216|6|Mentioned|p209|||Informal name.||||||
36885|Cooragoora Formation|23415|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group. Geological province: Pilbara Craton. Fine- to coarse-grained sandstone, siltstone, shale, conglomerate, and feldspathic and lithic wacke; weakly metamorphosed.||||||07-NOV-08
36885|Cooragoora Formation|23757|4|Described|p12-13|Archean|Archean|Upper part of De Grey Group. Conformable over Cattle Well Formation; unconformable below Callaw Formation. Max. thickness: >2000m. Predom. red to red-brown, medium- to coarse-gr. sst, pebbly sst, lithic wacke + matrix-supported polymictic conglom.||||||07-NOV-08
36885|Cooragoora Formation|23783|5|Briefly described|p10 Fig. 5|Archean|Archean|Of the De Grey Group?||||||07-NOV-08
36885|Cooragoora Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: ~2000m.  Interbedded sandstones, conglomerate, shale, siltstone and grey-brown wacke.  Geological Province: Pilbara Craton.||||||07-NOV-08
36885|Cooragoora Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: De Grey Group. Geological Province: Pilbara Craton||||||07-NOV-08
36885|Cooragoora Formation|24184|5|Briefly described|p699 Fig.3, p701|Archean|Archean|Of the De Grey Group. Geological Province: Pilbara Craton.||||||07-NOV-08
36885|Cooragoora Formation|50189|4|Described|p18|Archean|Archean|Of the De Grey Group; together with the Cattle Well Formation, replaces the Lalla Rookh Sandstone. Coarse to medium-grained sandstone, conglomerate; interbedded with siltstone and wacke. Conformably overlies: Cattle Well Formation.||||||07-NOV-08
36885|Cooragoora Formation|50544|3|Fully described|p35, p21 Tb. 4|Archean|Archean|Of the De Grey Group (Pilbara Supergroup).  Sandstone, polymictic conglomerate, siltstone, carbonaceous shale.  Conformably overlies Cattle Well Formation.  Max. thickness: ~2000m.||||||07-NOV-08
36885|Cooragoora Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Group (Pilbara Supergroup).  Fine to coarse-grained sandstone, siltstone, shale, conglomerate, and feldspathic and lithic wacke.  Geological Province: Pilbara Craton.||||||07-NOV-08
36885|Cooragoora Formation|60429|4|Described|p18|Archean|Archean|Of De Grey Group. Together with Cattle Well Fm., previously mapped as Lalla Rookh Sandstone. Conformably overlies Cattle Well Formation. Comprises coarse- to medium-grained sandstone, feldspathic sandstone and pebble to cobble conglomerate.||||||07-FEB-11
36885|Cooragoora Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the De Grey Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
36885|Cooragoora Formation|63441|5|Briefly described|p6 Tb. 1, p29|Archean|Archean|Formerly of De Grey Group in the Goldsworthy Basin. Now part of undivided Croydon Group in the Mallina Basin. Name abandoned.||||||07-FEB-11
36885|Cooragoora Formation|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Of Budjan, Cattle Well, Goldsworthy, Lalla Rookh, and Mosquito Creek Basins.||||||
39237|Cooterunah Group|23980|14|Not recorded|p291|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
24875|Cooya-Pooya-Gidley Granophyre|30766|6|Mentioned|p24|||Basic complex||||||
81573|Copernicus Intrusion|71873|5|Briefly described|p427-428|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Also known as Copernicus pyroxenite in Table 1, p431, p431, 433.|1823+/-3 Ma U-Pb SHRIMP crystallisation age||||Pyroxenite-peridotite body.|03-SEP-19
27378|Copley Formation|38263|6|Mentioned|p16|||||||||
27378|Copley Formation|39796|6|Mentioned|Map legend|Devonian|Devonian|||||||
27378|Copley Formation|44403|2|Defined|opp.p.6, Tb.1||Famennian|E/51-12, interbedded clastic limestone, oolitic limestone, sandy and silty limestone, limestone breccia. Famennian age.||||||
27378|Copley Formation|44404|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
27378|Copley Formation|44998|14|Not recorded|p.34-7||Frasnian|Interfingers with Pillara Formation. Overlies Pillara Formation. Frasnian goniatites. On many pages. p.25,26,41,47-9.||||||
27378|Copley Formation|45153|6|Mentioned|App.3-46|||||||||
28475|Copley Formation""|36890|6|Mentioned|p331|||||||||
41145|Copper Gorge Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||07-NOV-08
41145|Copper Gorge Formation|61253|5|Briefly described|p51, p56|||Consists of pillowed basalt and komatiitic basalt.  In unconformably contact with Warrawoona and Kelly Groups; and in fault contact with De Grey Supergroup.  Unconformably overlain by Nullagine Group rocks. Geological Province: Pilbara Craton.||||||30-AUG-05
41145|Copper Gorge Formation|61264|5|Briefly described|p64 Fig. 2|||Of the Pilbara Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||
41145|Copper Gorge Formation|63441|4|Described|p6 Tb. 1, p20|Archean|Archean|Obsolete - reassigned to Euro Basalt (Kelly Group). Prev.included in Mosquito Creek Fm (Warrawoona Gp) and Mt Roe Basalt (Fortescue Gp). Comprised pillowed basalt, komatiitic basalt, amphibolite, schist, chert, conglomerate+sst+siltstone+rare felsic tuff.||||||07-FEB-11
41145|Copper Gorge Formation|63854|5|Briefly described|p229 Fig.2|||||Of the Pilbara Supergroup.||||
41145|Copper Gorge Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Pilbara Supergroup. Geological Province: Pilbara Craton. Basalt, generally pillowed; minor massive komatiitic basalt; metamorphosed.||||||07-FEB-11
41145|Copper Gorge Formation|65008|3|Fully described|p7, p8, p13, p17, p41|Paleoarchean|Paleoarchean|New name. East Pilbara Granite-Greenstone Terrane. Type location: southern McPhee greenstone belt (between MGA 219850E 7600000N and 222600E 7601800N). Includes rocks previously part of the Warrawoona Group, Mosquito Creek Basin, and Mount Roe Basalt.|3315-2926 Ma|Of the Pilbara Supergroup||Unconformably underlain by the Warrawoona Group and Mosquito Creek Formation?|Basalt; generally pillowed; minor massive komatiitic basalt; metamorphosed.|
35644|Copper Hill Metamorphics|23152|5|Briefly described|p71|||||||||
41454|Copperhead "carbonatite"|50437|6|Mentioned|p4.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Age: 1821 +/- 4Ma (SHRIMP). Of the Speewah Group. Informal.||||||09-FEB-23
31893|Copperhead Albitite 'Carbonatite' Complex|22661|4|Described|p 299||Neoproterozoic|860 - 800 Ma.  See Copperhead Complex.||||||
31893|Copperhead Albitite 'Carbonatite' Complex|43854|5|Briefly described|Map Legend||Proterozoic|Age approx. ?1820 Ma.||||||
31893|Copperhead Albitite 'Carbonatite' Complex|44868|5|Briefly described|Map Legend||Proterozoic|||||||
80057|Copperhead Carbonatite|63866|5|Briefly described|p132, p138|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1821 Ma|Sally Downs Supersuite||||
34293|Copperhead Complex|22661|4|Described|p 312|||Has undergone at least one deformational phase p312.  See Copperhead Albitite 'Carbonatite' Complex.||||||
34475|Copperhead carbonatite|22754|6|Mentioned|p22|||Intruded the Tickalara Metamorphics.  Age: c.?1820Ma (Tyler et al, 1997b).||||||
34475|Copperhead carbonatite|70154|5|Briefly described|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic|Sample ID 94526040. Halls Creek Province. Data migrated from OZCHRON1. Original comment: 'The ages of the zircon suites are complex, with 1821 Ma being the interpreted magmatic age from 28 analyses. A lower Th/U group is older (1840-1880 Ma) and late Archaean xenocryst cores are 2419-2736 Ma.'|1821+/-4 Ma  U/Pb SHRIMP|||||
80035|Corboy Sandstone|67130|5|Briefly described|p16, p15 Fig10|Paleoarchean|Paleoarchean|||Soanesville Group||Overlies Cardinal Formation, overlain by Paddy Market Formation|Coarse clastic rocks.|20-SEP-17
24877|Cordalia Sandstone|22817|5|Briefly described|p2|Early Permian|Early Permian|Wooramel Group||||||
24877|Cordalia Sandstone|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
24877|Cordalia Sandstone|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Wooramel Group.||||||
24877|Cordalia Sandstone|23403|4|Described|p8|Early Permian|Early Permian|Of Wooramel Group.  Thinly bedded sandstone and siltstone.||||||24-NOV-09
24877|Cordalia Sandstone|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Wooramel Group.||||||
24877|Cordalia Sandstone|37294|6|Mentioned|p100|||||||||
24877|Cordalia Sandstone|37295|6|Mentioned|p51|||Proposed usage.||||||
24877|Cordalia Sandstone|40617|6|Mentioned|Fig.1|||||||||
24877|Cordalia Sandstone|41271|3|Fully described|p81|||Formerly "Cordalia Greywacke"||||||
24877|Cordalia Sandstone|41438|6|Mentioned|p104|||See also Fig.11||||||
24877|Cordalia Sandstone|42116|4|Described|p27|||||||||
24877|Cordalia Sandstone|42462|5|Briefly described|p56|||lateral equiv. to Nunnery Sandstone.||||||
24877|Cordalia Sandstone|69547|6|Mentioned|p196|||Southern Carnarvon Basin.||||||
24877|Cordalia Sandstone|72910|6|Mentioned|p20, p22, p34|Artinskian|Artinskian|Ref Hocking et al., 1987. Name replaced by Cordalia Formation.||||Underlies Moogooloo Sandstone.|Includes Sandstone.|18-FEB-21
77181|Core Sandstone""|44139|6|Mentioned|p280, p281 Table 3-15|||Telfer Dome. Informal name used by Blockley (1974) after unpublished work by Newmont P/L. Subsequently the Malu Quartzite.| | ||||05-MAR-18
40819|Cornelia 'Formation'|50188|6|Mentioned|p13|||Informal - see Cornelia Formation.||||||16-JUL-08
26497|Cornelia Formation|22589|6|Mentioned|p125||Proterozoic|||||||
26497|Cornelia Formation|22816|5|Briefly described|p8 Table 1|Neoproterozoic|Neoproterozoic|Of the Savory Group.||||||17-JUL-08
26497|Cornelia Formation|42708|5|Briefly described|Plate 1|Proterozoic||Variation on Cornelia Sandstone.||||||
26497|Cornelia Formation|43229|5|Briefly described|Map Legend||Mesoproterozoic|of Bangemall Group||||||
26497|Cornelia Formation|43492|3|Fully described|9,11|||||||||
26497|Cornelia Formation|43756|6|Mentioned|Fig.1,p534|||||||||
26497|Cornelia Formation|50188|5|Briefly described|p9, 12-13, Table 1.|||Of Williams (1992) to supersede Cornelia Sandstone. Name now disused and rocks divided into: Oldham Sandstone, Quadrio Formation and Cornelia Sandstone (now redefined). Of the Kahrban Subgroup. Geol. Prov: Bangemall Basin||||||16-JUL-08
26497|Cornelia Formation|61732|6|Mentioned|p88|||Probably unconformably overlain by, or faulted against, the Boondawari Formation in the trainor Hills area.||||||07-FEB-11
26497|Cornelia Formation|64283|5|Briefly described|p49|||Formerly "Cornelia Sandstone".Sandstone within this unit are differentiated based on changes in bedding orientation, hence revision of the unit to create Cornelia Sandstone, Oldham Sandstone and Quadrio Formation. Cornelia "Formation" mentioned (p51).||||||07-FEB-11
26497|Cornelia Formation|64286|5|Briefly described|p72|||Of Williams (1990, 1995). This represents a redefined and more restricted section of the former Cornelia Sandstone. Geological province: Oldham Inlier.||||||07-FEB-11
26497|Cornelia Formation|64772|5|Briefly described|p13|||Initially mapped by Brakel and Leech(1980) as Cornelia Sandstone, then as Cornelia Formation by Williams (1992, 1995a); later subdivided by Hocking et al (2000a,b) into Oldham Sandstone, Quadrio Formation and Cornelia Sandstone. Age: <1670Ma.||||||19-APR-13
26497|Cornelia Formation|64970|6|Mentioned|p719 Fig. 2, p722|Riphean|Riphean|Geological Province: Officer Basin.||||||27-MAY-09
26497|Cornelia Formation|65368|5|Briefly described|p13, p15 Fig. 1, p16 Fig. 2|Neoproterozoic|Neoproterozoic|Grey quartzites.||||||19-MAR-12
26497|Cornelia Formation|67454|5|Briefly described|pp563-567. |||Officer Basin. Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed.||||Is unconformably overlain by Browne Formation.|Well-cemented, medium-grained, cross-bedded sandstone.|
74602|Cornelia Sandstone""|64283|5|Briefly described|p49|||Of Brakel and Leech (1980). Superseded by Cornelia Formation (Williams 1992). Geological Province: Oldham Inlier.||||||07-FEB-11
34599|Cornelia""Formation|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Savory Sub-Basin||||||17-JUL-08
75887|Corner Well Gabbro|68287|5|Briefly described|Map Legend|Mesoarchean|Archean|Shown on map key at ~ same age as Kantie Murdana Volcanics Member, but no indication of any direct dating.|~ 2813 Ma|Of the Windimurra Igneous Complex.|||Olivine orthopyroxenite interlayered with anorthosite; metamorphosed.|
75887|Corner Well Gabbro|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Neoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane||Windimurra Igneous Complex|Includes 9 unnamed subunits.||Dunite with relict olivine cumulate texture; Leucocratic peridotite; Anorthosite; Clinopyroxene cumulate gabbro; Pyroxene cumulate gabbro; Olivine gabbro; Gabbronorite; Melanocratic norite|
75887|Corner Well Gabbro|69583|5|Briefly described|p54, p56, p99, p101, p103; Plate 2|Mesoarchean|Mesoarchean|Intrudes the lower and middle zones of the Complex.|c.2813 Ma.|Windimurra Igneous Complex.|||A late phase of gabbroic pipes <1 km in diameter; modally layered olivine gabbro interlayered with lherzolite; metamorphosed.|
75887|Corner Well Gabbro|69626|5|Briefly described|map legend|Archean|Archean|Murchison Domain, Youanmi Terrane, Yilgarn Craton||Windimurra Igneous Complex|||Interlayered olivine gabbro and leucogabbronorite.|
75887|Corner Well Gabbro|70419|5|Briefly described|p3, p7, p12, p24-25|Mesoarchean|Mesoarchean|Pipes are 0.3-2 km in diameter. May be comagmatic with the main lobe magmas; a final phase of low-volume primitive melt underlying the Complex.|c.2813 Ma.|Windimurra Igneous Complex.|||A late phase of peridotitic-gabbroic pipes.|
75887|Corner Well Gabbro|70796|5|Briefly described|100k_geologyl_lut.csv|Mesoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, Coolamaninu100_2540_stratig.pdf. Numerous additional lithologies are discussed.|ca 2813 Ma (inferred)|Meeline Suite|||Anorthosite, melanocratic gabbro to gabbronorite, locally with orthopyroxene cumulate crystals up to 20 mm; metamorphosed. Metamorphosed cumulate pyroxenite, clinopyroxene and olivine gabbros.|
75887|Corner Well Gabbro|70830|5|Briefly described|p30-31, p48|||Murchison Domain.|||||Peridotitic-gabbroic pipes, 0.3-2 km in diameter.|
75887|Corner Well Gabbro|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Of the Windimurra Igneous Complex. 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.|2813 Ma (inferred)|Unit of Meeline Suite.|||Dunite with relict olivine cumulate texture; grades into layers of troctolite, melanotroctolite and olivine gabbro; metamorphosed, olivine gabbro to olivine gabbronorite, olivine orthopyroxenite, clinopyroxenite cumulate gabbro, anorthosite.|
75887|Corner Well Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Youanmi Terrane.||Windimurra Igneous Complex|||Modally layered olivine gabbro grading into olivine gabbronorite interlayered with lherzolite, dunite, pyroxenite, and minor anorthosite; metamorphosed.|
39721|Corona Downs Granitoid complex|24188|6|Mentioned|p788 Fig.1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
68056|Corumup Gneiss|24526|5|Briefly described|p106 Fig. 7, p107|||Possibly misspelt? (place name is Coramup in WA). Ductile shear zone developed between the Coramup and Heyward Faults at the SE margin of the Biranup Complex.||||||02-MAR-05
68056|Corumup Gneiss|64722|6|Mentioned|Fig. 2 p3-6, p18|Ecstasian|Statherian|Also spelt Coramup. A shear zone along the southern margin of the Biranup Complex, Albany-Fraser Orogen, consisting of components of the Dalyup Gneiss and 1300-1280 Ma granite.||||||
72996|Corunna Downs Granitic Complex|63142|6|Mentioned|p487|Archean|Archean|Age: ca 3.30Ga. Granites.||||||07-NOV-08
72996|Corunna Downs Granitic Complex|64405|5|Briefly described|p2 Fig. 1|||||||||07-FEB-11
72996|Corunna Downs Granitic Complex|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Granitoid rocks including feldspar-porphyritic microgranite; metamorphosed.||||||15-DEC-08
72996|Corunna Downs Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
72996|Corunna Downs Granitic Complex|65827|4|Described|p1, p9 Fig3, Tb.3 p12, p19, p29, p32|Mesoarchean|Paleoarchean|Bagas et al. (2004); formerly Corunna Downs Batholith (Hickman 1983) and Corunna Downs Igneous Complex (Sims and Carson 2001). Includes Carbana Monzogranite, Mondana Monzogranite. Intruded by Black Range Dolerite Suite. Trondhjemite, granodiorite and monzogranite with rare tonalite, syenogranite. c.3315-3290 Ma.||||||
72996|Corunna Downs Granitic Complex|66217|5|Briefly described|p32.||||||Includes Emu Pool Supersuite.||Largely undeformed, coarse-grained K-feldspar monzogranites.|
72996|Corunna Downs Granitic Complex|67197|6|Mentioned|p3|||East Pilbara Terrane.||||||
72996|Corunna Downs Granitic Complex|67270|6|Mentioned|p3|Archean|Archean|||||||
72996|Corunna Downs Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
72996|Corunna Downs Granitic Complex|68284|5|Briefly described|p7|Archean|Archean|Kelly greenstone belt, East Pilbara Terrane.||||Intrudes Apex Basalt, Panorama Formation (Warrawoona Group).||
72996|Corunna Downs Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
72996|Corunna Downs Granitic Complex|73598|6|Mentioned|p1208 Fig.1|||East Pilbara Terrane. Appears as Corunna Downs Granite Complex.||||||
34394|Corunna Downs Granitoid Complex|22715|6|Mentioned|p216|Archean|Archean|||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23755|6|Mentioned|p11|||||||||
34394|Corunna Downs Granitoid Complex|23780|5|Briefly described|p146|Archean|Archean|Age: ~3432+/-2 Ma||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23783|5|Briefly described|p18|Archean|Archean|||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23784|5|Briefly described|p70|Archean|Archean|||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23807|6|Mentioned|p108|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23813|5|Briefly described|p103|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|23895|5|Briefly described|p884 Fig.1, p904|||||||||
34394|Corunna Downs Granitoid Complex|23936|6|Mentioned|p16|||Geological Province: Pilbara Craton.||||||
34394|Corunna Downs Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3317-3307Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|24184|4|Described|p703, p707 Fig.8|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3313 +/- 9Ma||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|24531|6|Mentioned|p29|Archean|Archean|Age: 3315Ma.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|24590|5|Briefly described|p19, p28 Fig. 1.2|Archean|Archean|Mainly comprises granodiorite and biotite-monzogranite. Includes a granodiorite section in the nortern part referred to as the Northern Suite, Age: 3. 31Ga. See also p32 and p41.||||||07-FEB-11
34394|Corunna Downs Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p133, p142|||See also p146 Tb.2-21, p150 Fig.2-138, p152, p153 Fig.2-140, p155 Fig.2-142. |||Includes Mondana, Carbana Pool Adamellites.||Biotite monzogranites, biotite-hornblende monzogranites, biotite tonalite, granodiorite, gneiss and migmatite, greenstone (amphibolite, meta-volcanic rocks and meta-sedimentary schist).|
34394|Corunna Downs Granitoid Complex|50381|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|50427|5|Briefly described|p174|Archean|Archean|Age: 3315 Ma, some 3420 Ma rocks, Flanked by Panorama Formation and Euro Basalt.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|62576|5|Briefly described|p618 Fig. 1|||Geological province: Pilbara Craton. ||||||
34394|Corunna Downs Granitoid Complex|64326|6|Mentioned|p71 Fig. 1|Archean|Archean|Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
34394|Corunna Downs Granitoid Complex|64327|3|Fully described|p61, p62|Archean|Archean|Subdivided into 4 mappable groups: Gp.1: Nandingarra and Triberton Granodiorites, and unnamed tonalite; Gp.2: Carbana Monzogranite and unnamed granitoid rocks; Gp.3: Mondana Monzogranite; and, Gp.4: an unnamed syenite. Geol. Province: Pilbara Craton.||||||07-NOV-08
34394|Corunna Downs Granitoid Complex|64328|6|Mentioned|p53|||||||||07-FEB-11
34394|Corunna Downs Granitoid Complex|64653|5|Briefly described|Map Legend|Archaean|Archaean|Includes Boobina Porphyry, Mondana Monzogranite and Carbana Monzogranite.||||||07-FEB-11
34394|Corunna Downs Granitoid Complex|65008|4|Described|p2, p5, p7-9, p11-p15, p24-26, p41  |Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Comprises an ovoid shaped body that tapers towards the southwest. Subdivided by Bagas et al. (2003, 2004a).|3317-3313 Ma||Includes Nandingarra Granodiorite, Carbana Monzogranite, Triberton Granodiorite, Mondana Monzogranite, and Boobina Porphyry.|Intrudes the Warrawoona Group.|Dominated by monzogranitic compositions, but also includes rare tonalite, trondhjemite, granodiorite, and syenite.|
34394|Corunna Downs Granitoid Complex|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|||Includes Carbana Monzogranite and Mondana Monzogranite.|||
34394|Corunna Downs Granitoid Complex|69167|6|Mentioned|178001.1.pdf|Archaean|Archaean|Age derived from sample of biotite monzogranite (178001.1.pdf) and is representative of a syenitic unit within the carbana monzogranite.|3310 +/- 4 Ma (SHRIMP)|||||
78449|Corunna Downs Igneous Complex|65827|6|Mentioned|p15|||The name by which the Corunna Downs Granitic Complex is referred in Sims and Carson (2001).||||||16-OCT-13
32595|Corunna Downs granite|45923|14|Not recorded|p.49,138|||||||||
38970|Corunna Downs granitoid complex|23807|6|Mentioned|p137|||Informal - see Corunna Downs Granitoid Complex.  Geological Province: Pilbara Craton.||||||
38970|Corunna Downs granitoid complex|24193|5|Briefly described|p874 Fig.1, p888|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38970|Corunna Downs granitoid complex|24590|6|Mentioned|p35, p132 Fig. 4.2|||Informal - see Corunna Downs Granitoid Complex. Mount is Mt in text.||||||07-FEB-11
81289|Coryie Formation|69547|5|Briefly described|p193|Artinskian|Artinskian|Southern Carnarvon Basin.||Unit of Byro Group.||Overlain by Mallens Formation. Underlain by Billidiee Formation.||
79471|Cosmo Newbery Dyke Suite|68186|5|Briefly described|p30, Plates 1A, 2|Phanerozoic|Proterozoic|NE Albany-Fraser Orogen and adjacent Eastern Goldfields Superterrane. Only recognised in aeromagnetic data.|||||NW-trending mafic dykes; interpreted from aeromagnetic data.|
79471|Cosmo Newbery Dyke Suite|70802|5|Briefly described|GEOL_LUT_CSV files|Cambrian|Proterozoic|Geological province: Albany-Fraser Orogen. Events: Western Australian events (4000-0.01 Ma). See 2_5m_interpdykel15_lut.csv, 250k_pre_mesozoic_interpgeol_lut.csv.|2500-510 Ma (inferred)||||Northwest-trending mafic dykes; interpreted from aeromagnetic data|
79471|Cosmo Newbery Dyke Suite|70826|6|Mentioned|p14 tbl 5|||Yilgarn Craton. Age ranges from 2500-510 Ma [not very useful].||||||
79471|Cosmo Newbery Dyke Suite|71270|4|Described|2_5m_interpdykel15_lut.csv|Cambrian|Proterozoic|Geological province: Yilgarn Craton, West Australian Craton. Events: Western Australian events (4000 - 0.01 Ma).|2500-510 Ma (inferred)||||Northwest-trending mafic dykes; interpreted from aeromagnetic data|
79471|Cosmo Newbery Dyke Suite|71493|5|Briefly described|p39, p44, p46|||Yilgarn Craton. NW trending dyke suite, defined from magnetic surveying and does not outcrop, has not been directly dated. Spatial relationship with ~600 Ma U-Pb disturbance. Map constraints indicate emplacement between 2500 Ma and 510 Ma (Spaggiari et al., 2011). Cosmo Newbery Dykes also used p42, p44.||||||
72624|Cossigny Formation|62837|5|Briefly described|Stratigraphic columns|Late Triassic|Late Triassic|Age: ~233Ma. Geological Province: Dampier Sub-basin, Rankin Platform, Beagle Sub-basin and Bedout Sub-basin (Roebuck Basin).||||||
73777|Cotter Bore pegmatite|50542|6|Mentioned|p118|||Informal name.||||||07-FEB-11
24882|Cottesloe Soil|40367|6|Mentioned|p76|||Of McArthur and Bettanay (1960).||||||07-AUG-07
68678|Coulter Sandstone|24173|6|Mentioned|p23|||Possible correlative of the Kimberley Group.||||||
78497|Counterunah Subgroup|67668|6|Mentioned|p155 Fig. 2||Paleoarchean|East Pilbara Terrane, Pilbara Craton. [misspelt Coonterunah Subgroup]||Warrawoona Group|Double Bar, Coucal, Table Top Formations.|||07-NOV-13
81298|Courlbarloo tonalite|70020|5|Briefly described|p118|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton.||Unit of Mount Kenneth Suite.||||
38686|Cowaramup Bay leucogabbro|23788|6|Mentioned|p22|||Geological Province: Yilgarn Craton.||||||
24884|Cowaramup Conglomerate|23816|6|Mentioned|p256|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
24884|Cowaramup Conglomerate|36890|5|Briefly described|p256|||||||||
32965|Cowaramup Conglomerate""|44303|14|Not recorded|p.14|||(ref. to Fairbridge & Teichert 1953). (I/50-5,9).||||||
38673|Cowaramup gneiss|23788|5|Briefly described|p8|||Informal unit of the Leeuwin Complex. Parent: Leeuwin Complex. Geological Province: Yilgarn Craton.||||||
34231|Cowarna Rocks|22672|6|Mentioned|P269||Siderian|Age of unit is 2400 Ma||||||
24232|Crispin Conglomerate|12099|6|Mentioned|p678 Fig.4|||Placed in Glengarry Group by Gee (1987)||Unit in Glengarry Group.||||04-MAR-13
24232|Crispin Conglomerate|35975|4|Described|p100|||||||||
24232|Crispin Conglomerate|40938|6|Mentioned|Fig.5|||||||||
24232|Crispin Conglomerate|40989|5|Briefly described|p13|||||||||
24232|Crispin Conglomerate|49896|5|Briefly described|p2 Tb. 1|||||||||
24232|Crispin Conglomerate|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Glengarry Basin/Group (Gee 1987)||||||
24232|Crispin Conglomerate|65419|5|Briefly described|pp5-6.|Paleoproterozoic|Paleoproterozoic|Of Gee (1987). Now recognized as a mylonitic unit and not stratabound, hence cannot be regarded as a Formation. Now considered part of the Peak Hill Schist; more appropriately referred to as Crispin Mylonite.|||||Quartzite clasts in a matrix of quartz-sericite schist; both mylonitized.|
24232|Crispin Conglomerate|70804|6|Mentioned|p2, p23|||Obsolete name.||||||
24232|Crispin Conglomerate|71484|5|Briefly described|p122,124,126,133|Rhyacian|Rhyacian|Fairly coherent, deformed and metamorphosed up to amphibolite-grade. Maximum depositional age of 2170+\-18 Ma (SHRIMP; Wingate et al., 2014a,b), possibly coeval in deposition with Juderina Formation.||Unit of Peak Hill Schist.|||Quartz pebble to cobble conglomerate.|30-AUG-19
37100|Crispin conglomerate|23747|5|Briefly described|p4|||Informal.||||||
31378|Cronin Formation|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
31378|Cronin Formation|43563|6|Mentioned|Fig.2,p5||Early Cretaceous|Misspelling/variation of Cronin Sandstone||||||
31378|Cronin Formation|43656|6|Mentioned|Fig.2,p8|Barremian|Berriasian|||||||
31378|Cronin Formation|43746|6|Mentioned|Fig.2,p11|Barremian|Berriasian|||||||
31378|Cronin Formation|44143|4|Described|p.432 Table 4-19; p.449, Figure 4-108|Cretaceous|Jurassic|Up to 50m thick; fine to coarse sandstone; fluvial. Unconformably overlies Paterson Formation; disconformably overlain by Anketell Sandstone. Type section at Cronin Hills (RUNTON: 23deg 14' S, 123deg 23' E). Appears as Cronin Sandstone in Fig.4-108.||||||23-NOV-17
31378|Cronin Formation|44998|14|Not recorded|p.120|||||||||
31378|Cronin Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
31378|Cronin Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
31378|Cronin Formation|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Is overlain by Samuel Formation. Lateral equivalent of Broome Sandstone.||
31378|Cronin Formation|68007|6|Mentioned|p4|Cretaceous|Cretaceous|Canning Basin.||||||
31378|Cronin Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlain by Samuel Formation.||
31378|Cronin Formation|69182|6|Mentioned|Ch4 p9, Ch4 p45, Ch4 p47, |Early Cretaceous|Early Cretaceous|Canning Basin. ||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Samuel Formation.||10-FEB-20
31378|Cronin Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Samuel Formation. Equivalent to the Broome Sandstone and the Callawa Formation.||10-FEB-20
31378|Cronin Formation|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Unconformably overlies the Jarlemai Formation, Overlain by the Samuel Formation.|Sandstone, shale and conglomerate.|10-FEB-20
31378|Cronin Formation|72497|5|Briefly described|p3 Fig.2.|Barremian|Berriasian|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins.||||Conformably underlies Samuel Formation and is laterally equivalent to Callawa Formation. Unconformably overlies Jarlemai Siltstone.||
31378|Cronin Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Willara Sub-basin.||||Shown with Callawa Formation as unconformably overlying Jarlemai Formation, underlies Samuel Formation and is laterally equivalent to Broome Sandstone.||
31378|Cronin Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin. Lower boundary[?] marked by the Breakup Unconformity that represents Jurassic-Cretaceous extensional events offshore.||||Unconformably underlain by Jarlemai Siltstone. Overlain by Samuel Formation. Equivalent to Callawa Formation and Broome Sandstone.|Dominantly sandstone with lesser shale and conglomerate in the lower portion[?].|
83162|Crossing Bore Schist|70094|6|Mentioned|p80|||Detrital zircons from this and other units were analysed to establish similar provenances for Harts Range Group, Amadeus and Georgina Basins.||||||
80186|Crossroads Monzogranite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Big Bell Suite.|||Late-volcanic granite.|
80186|Crossroads Monzogranite|70030|5|Briefly described|p191|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Big Bell Suite.||||
80186|Crossroads Monzogranite|70830|6|Mentioned|p8|||Murchison Domain. ||||||
25866|Crown Basalt Member|30562|2|Defined|p39|Archean|Archean|See also P37||||||07-NOV-08
37472|Crystal Rich Tuff|24041|5|Briefly described|p493|Archean|Archean|Of Wittenoom Dolomite. Geological Province: Pilbara Craton||||||07-NOV-08
29990|Crystal-rich Tuff|22689|6|Mentioned|138,139,141|Paleoproterozoic|Archean|Of Bee Gorge Member, Wittenoom Formation, Hamersley Basin. SHRIMP age 2561+/-8 Ma. Mulitgrain age of Hassler (1991), 2603 Ma+/- 7 Ma||||||07-NOV-08
29990|Crystal-rich Tuff|43064|5|Briefly described|p69|||Informal stratigraphic unit of Bee Gorge Member. Radiometric age 2603 +/-7Ma||||||
80620|Crystalline Limestone""|65942|6|Mentioned|p74|||Of Tate (1879).||||||
39659|Cudalgarra member|24449|6|Mentioned|p745|||Informal - see Cudalgarra Member.||||||
83142|Cue Gabbro|72491|6|Mentioned|p5 Fig.4|||Murchison Terrane, Yilgarn Craton.||||||
28487|Culdiva Sandstone|34010|6|Mentioned|Cor. chart|||Mis-spelling of Culvida.  M.Trias.||||||
28487|Culdiva Sandstone|46863|6|Mentioned|p25|||||||||
28487|Culdiva Sandstone|64643|5|Briefly described|p9|Triassic|Triassic|Up to 200m of fine to coarse-grained sandstone and conglomerate.||||||24-NOV-08
77445|Cullens Diamicrite|60386|6|Mentioned|p296, 309|Asselian||Southern Perth Basin. Non-marine.||||||
74638|Cullens Diamictite""|22820|5|Briefly described|p8-9 Tbs. 1&2,  p11|Early Permian|Early Permian|An irregular argillaceous unit at base of the Stockton Group succession. Name used in parenthesis in tables 1 and 2; and informally in text - since there has been insufficient thickness intersected in boreholes to warrant formal naming.||||||11-AUG-08
74638|Cullens Diamictite""|70774|5|Briefly described|p5 fig 3|Asselian|Asselian|Southern Perth Basin. Actually shown as 'Cullens Diamictite'.||||Overlain by the Mosswood Formation.||
34991|Cummins Range Carbonatite|23040|6|Mentioned|p151||Archean|||||||07-NOV-08
34991|Cummins Range Carbonatite|24540|6|Mentioned|p4|||Vermiculite resource in WA.||||||07-FEB-11
34991|Cummins Range Carbonatite|67127|5|Briefly described|p106, p126, p128, p136, p171, p189-190|Tonian|Stenian|Halls Creek orogen, WA. Pre-dates kimberlites of the Kimberley region. Potentially co-eval with the Bow-Hill lamprophyres. Associated with a regolith-sourced radiometric anomaly. Forms a sub-vertical, zoned stock located near the junction of the Halls Creek and King Leopold orogens.|1012 +/- 12 Ma (U-Pb zircon); 905 +/- 2 Ma (Rb-Sr)||||Carbonatite capped by silicified, limonitic collapse breccia, enclosed by carbonated, mica-rich pyroxenite.|08-FEB-23
34991|Cummins Range Carbonatite|70826|6|Mentioned|p13|||Southern Halls Creek Orogen.||||||08-FEB-23
28489|Cundlego "Series"|38917|6|Mentioned|p162|||||||||
42385|Cundlego Sandstone""|23815|6|Mentioned|p286|||Superseded by the Cundlego Formation (Condon 1954).||||||13-DEC-04
78195|Cunyu Sill|62289|6|Mentioned|p9 Fig. 6|||dolerite. Shown in generalised section of Juderina Formation which has been thickened by intrusion of dolerite sills.||||||
32873|Curdamurda Sandstone|48848|14|Not recorded|p.13|||Mis-spelt?||||||
39738|Curlew pegmatite|24193|5|Briefly described|p876|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
79550|Cyclops Formation|67128|6|Mentioned|p30|||Northeastern Amadeus Basin.||||||
40322|D. lobispinosum sand member|50024|6|Mentioned|p13|||Informal name.  See also D. lobispinosum sands.  Hosts recoverable oil.  Geological Province: Carnarvon Basin.||||||
40321|D. lobispinosum sands|50024|5|Briefly described|p13|Early Cretaceous|Early Cretaceous|Informal name.  See also D. lobispinosum sand member.  Hosts recoverable oil, sealed by B. reticulatum shales.  Geological Province: Carnarvon Basin.||||||
41038|D.C. Basalt|24196|5|Briefly described|p47 Fig.5|||Initials probably stand for Devon Consols Basalt. Overlain by Kapai Slate. Overlies the Kambalda Komatiite. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||28-MAY-04
41038|D.C. Basalt|64633|6|Mentioned|p4 Fig.3, p6 Fig.4.|||Kalgoorlie Terrane.||Unit in Kambalda Sequence.||||
41038|D.C. Basalt|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. ||Unit of Kambalda Sequence.||Ovelain by Kapai Salte. Underlain by Kambalda Komatiite.|Basalt.|
41038|D.C. Basalt|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Kambalda Komatiite. Overlain by the Kapai Slate.||
41038|D.C. Basalt|72485|6|Mentioned|p3 Fig.2|||||Kambalda Sequence.||||
41038|D.C. Basalt|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
81299|Dairy monzogranite|70020|6|Mentioned|p122|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.|2679+\-2 Ma|||||
24900|Dales Gorge Member banded iron-formation|36247|6|Mentioned|Fig.3|||||||||
68724|Dales Gorge Member shales|60706|6|Mentioned|p624|||Informal - see Dales Gorge Member||||||
70356|Dales Gorge Shale Member|61577|5|Briefly described|p786 Fig. 1B|Archean|Archean|Possibly misspelt - see Dales Gorge Member. Age: ca2.50-2.470GA.  Geological Province: Hamersley Basin.||||||07-NOV-08
70209|Dales Gorge spherule layer|61576|5|Briefly described|p774 Fig. 1|||Of the Hamersley Group. Geological Province: Hamersley Basin. Appears as Dales Gorge SL in figure. See also p779. ||||||
70209|Dales Gorge spherule layer|70733|6|Mentioned|p116, 119|||Comparison of PGE values with Marble Bar Chert Member. Appears only as Dales Gorge.||||||
75774|Dalgaranga Supersuite|65545|6|Mentioned|Bedrock geology|||Gascoyne Province. See also Dalgaringa Supersuite||||||
83143|Dalgarangado igneous complex|72491|6|Mentioned|p5 Fig.4, p56|||Murchison Terrane, Yilgarn Craton. Appears merely as Dalgarangado in Fig.4.|~2727 - 2720 Ma.|||||
68838|Dalgeringa Supersuite|23780|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|Age: ~1800+/-7 Ma||||||07-NOV-08
74120|Dalgety Gneiss|24197|6|Mentioned|p69|||Of Williams (1986). Informally referred to as the Dalgety Gneiss dome, parts of which are incorporated into the Minnie Creek Supersuite.||||||07-FEB-11
74120|Dalgety Gneiss|66299|6|Mentioned|p73.|||Used in the term Dalgety Gneiss Dome (Williams 1986), an informal name for a granodiorite equivalent to the Nardoo Granite.|||||Gneissic biotite-hornblende granodiorite.|
39726|Daltons Suite|24185|5|Briefly described|p747|Archean|Archean|Geological Province: Pilbara Craton. Ultramafic sills, subvolcanic and Honeyeater Basalt of the Gorge Creek Group (van Kranendonk et al, 2002).||||||07-NOV-08
39726|Daltons Suite|67130|5|Briefly described|p16|||Emplaced alongside eruption of the Honeyeater Basalt|||||Dunite through to pyroxenite, dolerite and local granophyre.|
39726|Daltons Suite|72668|6|Mentioned|p6, p9, p28|||East Pilbara Terrane. [correctly] Spelt Dalton Suite p9.|C. 3200 Ma.||||Layered mafic to ultramafic intrusions ranging from dunite, through pyroxenite to dolerite with local granophyre.|13-JAN-22
70331|Daltons sandstone|61266|5|Briefly described|p60|||Informal name used by Boulter et al. (1987) to describe pebbly sandstones in a tectonic sliver of Gorge Creek Group and interpreted to be the equivalent Lalla Rookh Sandstone. Has been re-assigned to the Corboy Formation. Geol. Prov: Pilbara Craton.||||||
81300|Damperwah granite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Jungar Suite.||||
27757|Dampier Formation|23768|6|Mentioned|p145, p147|Late Pleistocene|Late Pleistocene|See also Dampier Limestone.||||||10-MAR-05
27757|Dampier Formation|23815|4|Described|p307|Middle Pleistocene|Middle Pleistocene|Formerly known as the "Dampier Unit". Geological Province: Carnarvon Basin. Underlain by Tamala Eolianite (disconformable). Max. thickness:1.2 m. Contains rich bivalve fauna.||||||13-OCT-08
27757|Dampier Formation|29721|6|Mentioned|p102|||||||||
27757|Dampier Formation|30693|6|Mentioned|p50|||||||||
27757|Dampier Formation|31604|6|Mentioned|p6|||Oxfordian to Tithonian. Table 6.||||||
27757|Dampier Formation|31949|5|Briefly described|p62|||||||||
27757|Dampier Formation|32711|6|Mentioned|Fig.3|||||||||
27757|Dampier Formation|32714|6|Mentioned|Fig.7|||Jurassic. Dingo Gp.||||||
27757|Dampier Formation|32715|6|Mentioned|Fig.16|||||||||
27757|Dampier Formation|35105|6|Mentioned|p4|||||||||
27757|Dampier Formation|36890|3|Fully described|p307|||||||||
27757|Dampier Formation|38954|6|Mentioned|Table 1|||||||||
27757|Dampier Formation|45142|6|Mentioned|Fig.10|||||||||
73576|Dampier Granitic Complex|63441|5|Briefly described|p37|Archean|Archean|Includes as part of its structure - Miaree Granite, Eramurra Monzogranite and Hearson Cove Monzogranite. The first two granites have an age range equal to that of Maitland River Supersuite, of 3000-2980Ma.||||||07-FEB-11
73576|Dampier Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
73576|Dampier Granitic Complex|67201|4|Described|p13 Fig.8, p25, p42|||In northwestern Pilbara Craton. 3140+/-40 Ma, Kiyokawa and Taira (1998). Nd TDM model ages on two granites are 3360-3330 Ma (Smithies et al. 2007).|c. 2990 Ma|||Probably intrudes Nickol River Formation (as source of veins in tectonic slices).|Granitic rocks; monzogranite.|22-NOV-16
73576|Dampier Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
73576|Dampier Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
31689|Dampier Granitoid Complex|22449|6|Mentioned|P28, Table3 P27||Archean|||||||07-NOV-08
31689|Dampier Granitoid Complex|23484|4|Described|p18|Archean|Archean|Age: ~2990Ma. Geological Province: Pilbara Craton||||||07-NOV-08
31689|Dampier Granitoid Complex|23570|5|Briefly described|p159|Archean|Archean|||||||07-NOV-08
31689|Dampier Granitoid Complex|23784|5|Briefly described|p10|Archean|Archean|||||||07-NOV-08
31689|Dampier Granitoid Complex|23789|4|Described|p12|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
31689|Dampier Granitoid Complex|23794|5|Briefly described|Map Legend|||||||||
31689|Dampier Granitoid Complex|24023|5|Briefly described|p20|Archean|Archean|||||||07-NOV-08
31689|Dampier Granitoid Complex|24184|4|Described|p712|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.2990Ma (Nelson 1998, 1999). Intrudes the Regal Formation; intruded by the Gidley Granophyre||||||07-NOV-08
31689|Dampier Granitoid Complex|24541|3|Fully described|p1, p12, p32-34|Archean|Archean|Geological Province: West Pilbara Granite-Greenstone Terrane. Age: substantial part is c. 2990 Ma. Unconformably overlain by the Fortescue Group in southwestern Dampier - Barrow Island, in Fortescue and in the Dampier Archipelago.||||||07-NOV-08
31689|Dampier Granitoid Complex|24543|5|Briefly described|Map legend|Archean|Archean|Age: c.2990Ma.||||||07-NOV-08
31689|Dampier Granitoid Complex|43822|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
31689|Dampier Granitoid Complex|44150|6|Mentioned|p130-131 Fig.2-130|||||||||
31689|Dampier Granitoid Complex|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton. Age: 2990 Ma||||||07-NOV-08
31689|Dampier Granitoid Complex|50430|4|Described|p164||Archean|3160-3060 Ma. May be derived from Karratha Granodiorite and/or lower Roebourne Group. Intrudes Regal Formation. In West Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
31689|Dampier Granitoid Complex|61268|6|Mentioned|p79|||||||||
38079|Dampier Granophyre""|23570|6|Mentioned|p159|||Replaced by Gidley Granopyhre.||||||
32725|Dampier Group|44479|2|Defined|Tb.1|||E/51-1. Correlates with Anketell Sandstone of this Sheet.||||||
32725|Dampier Group|44997|14|Not recorded|p.38|||||||||
42386|Dampier Unit""|23815|6|Mentioned|p307|||Superseded by the Dampier Formation (Logan, Read and Davies, 1970).||||||
39739|Dampier granitoid complex|24193|5|Briefly described|p874 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
28494|Dandaragan Series""|23816|6|Mentioned|p248|||Superseded by the Dandaragan Sandstone (Faibridge, 1953).||||||
28494|Dandaragan Series""|30188|6|Mentioned|p74|||Refs to Blatchford(1912). Amended Fairbridge(1953).||||||
28494|Dandaragan Series""|36890|6|Mentioned|p248|||Renamed Dandaragan Sandstone||||||
24902|Dangara Sandstone Member|31910|4|Described|p16|||||||||
38666|Danjo monzogranite|23786|5|Briefly described|p35 Tb. 4|||Informal name.  Geological Province: Yilgarn Craton.||||||
38666|Danjo monzogranite|24091|6|Mentioned|p66|||Informal - see Danjo Monzogranite.||||||
81301|Danjo syenogranite|70020|6|Mentioned|p122|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.||||||
38677|Darling Range Granite""|23788|6|Mentioned|p14|||Geological Province: Yilgarn Craton.||||||
73790|Darling Range bauxite|60556|5|Briefly described|p7-12|||||||||
72633|Darling Range granitoids|62842|6|Mentioned|p214|||Part of the Darling Range Batholith.||||||28-NOV-06
75189|Darwin Formation, Lower|5952|5|Briefly described|p222|||Informal. Name has been refered to as Lower Darwin Formation or Darwin Shale Member.||||||05-MAY-09
77470|Darwin Radiolarite|13267|6|Mentioned|p278 Fig.3.|||See Darwin Formation.||||||
77470|Darwin Radiolarite|69452|6|Mentioned|p36:22|Albian|Aptian|Geoscience Australia (2009, 2011), for the Darwin Formation.||||||12-JUL-16
77470|Darwin Radiolarite|69456|6|Mentioned|p40:6|||Geoscience Australia (2011), for the unit in offshore Bonaparte Basin equivalent to the Darwin Formation.||||||12-JUL-16
77470|Darwin Radiolarite|69689|6|Mentioned|p16|Triassic|Triassic|Bonaparte Basin.||||Overlies Echuca Shoals Formation.||
34218|Darwin Shale|22663|5|Briefly described|W97 -1- 7 Fig.3||Early Cretaceous|||||||
75190|Darwin Shale Member|5952|5|Briefly described|p222|||Name has been refered to as Lower Darwin Formation or Darwin Shale Member interchangably.||||||01-MAR-10
72646|Darwin/Echuca Shoals Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Late Jurassic|Informal compound term to include both the Darwin Formation and Echuca Shoals Formation. Age: ~137-115Ma. Geological Province: Londonderry High. Within the Bathurst Island Group.||||||09-NOV-06
41040|Day Rock granodiorite|24196|5|Briefly described|p40|Archean|Archean|Age: 2676 +/- 5 Ma (Nelson, 2000). Geological Province: Yilgarn Craton||||||17-FEB-14
69376|Daylight Well granodiorite|60981|5|Briefly described|p176|Archean|Archean|Informal - see Daylight Well Granodiorite.||||||07-NOV-08
38621|DeGrey Group|23784|5|Briefly described|p3 Fig. 1|Archean|Archean|Misspelt - see De Grey Group.  Age: 2980-2940Ma.||||||07-NOV-08
38621|DeGrey Group|23936|6|Mentioned|p27, Fig.4|||Misspelt - see De Grey Group.||||||
79033|Dead Bullock Beds|69618|5|Briefly described|p93 Fig.3, p102 Fig.13|||Newmont geologists' terminology. ~30m thick.||Unit in Callie Member.||Overlies Coora Dolerite. Is over by Schist Hills Iron Beds.|Massive to poorly bedded, quartz-feldspar-sericite-pyrite-graphite siltstone and claystone.|
79033|Dead Bullock Beds|69747|5|Briefly described|p266|||Geological province: Granites-Tanami Orogen. Occurs locally in association with Dead Bullock Soak goldfield.||Unit of Callie Member.||||
79033|Dead Bullock Beds|70024|6|Mentioned|p36 Fig.15||||||||Ferruginous pelite.|
81869|Dead Bullock Group|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. See also Dead Bullock Formation.(of Crispe et al; 2007).||Tanami Supergroup||||
41455|Dead Fish Tonalite|50437|5|Briefly described|p1.7, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Dougalls Suite. Possibly misspelt - refers to Dead Finish Tonalite?||||||07-NOV-08
35353|Deception Hill Porphyry|23531|4|Described|Fig 3 p7, p9.||| Age: 3023+/-10 Ma. (SHRIMP U-Pb zircon).||||||08-AUG-06
35353|Deception Hill Porphyry|23532|5|Briefly described|Map legend||Archean|Age: c.3023 Ma. Yilgarn Craton.||||||07-NOV-08
35353|Deception Hill Porphyry|23787|5|Briefly described|p12 Fig. 6|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
35353|Deception Hill Porphyry|24167|5|Briefly described|p30|Archean|Archean|Age: 3023+/-10Ma (SHRIMP U-Pb zircon: Nelson, 1999).||||||07-NOV-08
35353|Deception Hill Porphyry|24245|6|Mentioned|p14|||Geological Province: Yilgarn Craton.||||||
75505|Deeadeea Claystone Member|64630|6|Mentioned|p35 |||Of Carolyn Formation.||||||
74866|Deeadeea Member|64643|5|Briefly described|p8|Sakmarian|Sakmarian|Of Carolyn Formation. Abbreviation of Deeadeea Sandstone Member. See p18.||||||
41082|Defiance dolerite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain.  Of the Kalgoorlie Group.||||||07-NOV-08
80241|Depuch Formation (Carnarvon Basin)|23815|5|Briefly described|p308|Late Pleistocene|Middle Pleistocene|Geological Province: Carnarvon Basin. Max. thickness: 1.5 m.||||||
80241|Depuch Formation (Carnarvon Basin)|35105|6|Mentioned|p27|||||||||
80241|Depuch Formation (Carnarvon Basin)|36890|3|Fully described|p307|||||||||
80241|Depuch Formation (Carnarvon Basin)|38485|4|Described|p19|Pleistocene|Pleistocene||||||A thin unit of well-indurated red-brown calcarenite and calcirudite.|27-SEP-17
80241|Depuch Formation (Carnarvon Basin)|41271|5|Briefly described|p197|||||||||
40062|Depuch Trondjemite|23936|5|Briefly described|Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 3093-2925 Ma.||||||07-NOV-08
70445|Depuch trondhjemite|61267|6|Mentioned|p71, p73 Tb.1|||Informal name for trondhjemite that is unnamed and undated. Compositionally identical to c. 2925 Ma granite from Caines Well Granitoid Complex. Geological Province: Pilbara Craton.||||||
32169|Derby Group|43976|6|Mentioned|p69|||Re.geology.||||||
32169|Derby Group|44006|14|Not recorded|p65|||Made up of Erskine Formation and Blina Shale. See also Lexicon.`||||||
69628|Desert Brown granite|61273|6|Mentioned|p87|||Not intended as a formal stratigraphic name. Commercial name for dimension stone from the Esperance region.||||||
31862|Desert's Revenge 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
31862|Desert's Revenge Granite|50436|5|Briefly described|p1.3, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the Mount Crofton Group (O'Callaghans Supersuite).|||||syenogranite to alkali-feldspar|27-SEP-12
80316|Deserts Revenge Granite|67202|6|Mentioned|p206|||Geochemistry diagram.||||||
39343|Devil Consuls Basalt|24091|6|Mentioned|p44|||Geological Province: Yilgarn Craton.||||||
79526|Devon Consols basalt|62083|5|Briefly described|p1014 Fig.6|Neoarchean|Neoarchean|Main gold camp: Kalgoorlie.|2692 Ma|[said to be] Kambalda Group.|||Mafic volcanic rock.|01-SEP-16
28503|Devon Consuls Basalt|30882|6|Mentioned|p50|||Misspelling of Devon Consols.||||||
28503|Devon Consuls Basalt|67198|5|Briefly described|p83, p88, p133|||[Mis-spelling of Devon Consols Basalt] (see references to that unit on p5 Fig.2, p81, p83). 60-100m thick. Geochemistry detailed.|2651 +/- 12 Ma (maximum eruption age).|||Overlies Kambalda Komatiite. Is overlain by Kapai Slate.|Pillowed flows with felsic ocelli; massive komatiitic basalt with minor pillow phases.|
38792|Devon Consuls basalt|23926|6|Mentioned|p10 Tb. 1|||Misspelt and Informal.||||||
77735|Devons Consols Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Formal name is Devon Consols Basalt.|||||Komatiite and high MgO basalt.|
41041|Diary monzogranite|24196|5|Briefly described|p44|Archean|Archean|Age: 2680 +/- 2 Ma (Black et al., 2002). Geological Province: Yilgarn Craton.||||||07-NOV-08
40748|Diebel Subgroup|24183|5|Briefly described|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin. Of the Bangemall Group.||||||
28504|Diemals basalt|40302|6|Mentioned|p23|||||||||
28506|Ding Dong Downs Formation|32660|5|Briefly described|Table 1|||||||||
28506|Ding Dong Downs Formation|33443|6|Mentioned|p260|||||||||
28506|Ding Dong Downs Formation|41980|6|Mentioned|Fig.5 P587|||||||||
28506|Ding Dong Downs Formation|45047|6|Mentioned|p61|||Refers Smith J.W.||||||
24920|Dingo Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
24920|Dingo Complex|38461|5|Briefly described|p1583|||||||||
24920|Dingo Complex|42329|5|Briefly described|p4|||||||||
24920|Dingo Complex|43597|6|Mentioned|p716|||||||||
74000|Dingo Formation|12491|6|Mentioned|p454-456.|||Name replaced by Dingo Claystone. Dingo Formation used in figures. Dingo Claystone used in text.||||Overlies Calypso Formation. Is overlain by Dupuy Formation.||20-JAN-15
74000|Dingo Formation|14227|5|Briefly described|p11|Late Jurassic|Middle Jurassic|Geological Province: Exmouth Sub-basin. Marine shales.||||||07-FEB-11
74000|Dingo Formation|67368|6|Mentioned|p210 Fig.5. |||See Dingo Claystone.||||||
74000|Dingo Formation|69692|6|Mentioned|p4|Late Jurassic|Late Jurassic|Northern Carnarvon Basin.||||Overlies Calypso Formation. Is overlain by Barrow Group.||
34308|Dingo Granite (WA)|22484|6|Mentioned|p74|Statherian|Statherian|Zircon xenocryst age 1773 +/-7 Ma.||||||
34308|Dingo Granite (WA)|22660|4|Described|p 301||Paleoproterozoic|Local name given to the Granite.||||||07-NOV-08
34308|Dingo Granite (WA)|24183|5|Briefly described|p6|||Age: 1674 +/- 6 Ma.||||||
34308|Dingo Granite (WA)|50216|5|Briefly described|p213|Paleoproterozoic|Paleoproterozoic|Granular iron formation. H42 Of the northern Gascoyne Complex. Age: 1674 Ma (Nelson, 2002, Pearson et al., 1996).||||||28-FEB-13
34308|Dingo Granite (WA)|50225|6|Mentioned|p388, p397|||Superseded by Dingo Creek Granite.  Age: c.1674Ma (Pearson et al, 1996) - age may have been intended for Dingo Creek Granite and name was misspelt in this instance?||||||
34308|Dingo Granite (WA)|63869|5|Briefly described|p22, p23, p24, p27-29|||Pearson (1996); renamed Dingo Creek Granite "because of potential confusion with the Dingo intrusion in the Pilbara"; also for reasons of precedence.|1674 +/- 6 Ma SHRIMP U-Pb zircon (Pearson, 1996).|||||
34308|Dingo Granite (WA)|64329|6|Mentioned|p15|||||||||
34308|Dingo Granite (WA)|65830|6|Mentioned|p31|||Of Pearson (1996); subsequently Dingo Creek Granite.||||||
34308|Dingo Granite (WA)|66299|6|Mentioned|p252.|||Gascoyne Province. Name used by Pearson (1996) for a distinctive granite subsequently renamed Dingo Creek Granite.||||||
34308|Dingo Granite (WA)|68992|5|Briefly described|p505, p507|Statherian|Statherian||1674 +/- 6 Ma; 1679 +/- 6 Ma (SHRIMP Zircon ages)|||||07-MAR-18
69928|Dingo Granite""|61262|6|Mentioned|p450|||Of Pearson (1996). Superseded by Dingo Creek Granite. ||||||
38790|Dinky Buoys porphyry suite|23926|6|Mentioned|p9|||Informal.  Geological Province: Yilgarn Craton.||||||
41043|Diorite Hill layered noritic complex|24196|6|Mentioned|p11|||Informal name.||||||28-MAY-04
32755|Dirk Hartog Dolomite|45015|6|Mentioned|map legend||Silurian|Geological Province: Carnarvon Basin. See also Dirk Hartog Limestone.||||||29-JAN-08
32755|Dirk Hartog Dolomite|61958|5|Briefly described|Map sheet 1|Silurian|Silurian|||||||
37059|Dirk Hartog Sandstone|23726|5|Briefly described|p7 Fig 2b|Devonian|Devonian|Overlying unit Faure Formation. Underlying unit Tumblagooda Sandstone. Geological Province: Carnarvon Basin.||||||
37059|Dirk Hartog Sandstone|67200|5|Briefly described|p7 fig 5,|Devonian|Devonian|||||Overlies Tumblagooda Sandstone, overlain by Faure Formation|Parallel bedded sandstone, siltstone, limestone, dolomite and salt.|
41225|Discovery Chert Formation|50226|5|Briefly described|p426|||Of the Edmund Group (Bangemall Supergroup).  An important stratigraphic marker.  Predominantly silicified carbonaceous siltstone.||||||24-JUN-04
69382|Discovery granodiorite|60980|5|Briefly described|p142 Fig.2, p145|||Informal name||||||
73860|Dixon Pillow Basalt|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Cleaverville Group. Informal name. Thick pillow basalt forming top section of the underlying Dixon Island Formation. Overlain by Snapper Beach Formation. Geological Province: Pilbara Block.||||||07-NOV-08
73860|Dixon Pillow Basalt|68574|6|Mentioned|p4|||Kiyokawa and Taira (1998), for a previously unnamed part of the Cleaverville Formation. Crops out along N coast of Dixon Island with intermittent exposures along Cleaverville Beach. The name is invalid (reasons given); the rocks are renamed the Port Robinson Basalt, included in the Regal Formation (Ryan and Kriewaldt, 1964).||||||
29414|Dixon Range beds|22561|4|Described|p15|||||||||
29414|Dixon Range beds|22567|6|Mentioned|p91|||||||||
29414|Dixon Range beds|42940|5|Briefly described|Plate 2|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, slate, tuff, basalt, felsic porphyry and metamorphic equivalents.  Geological province: Amadeus Basin.||||||07-NOV-08
29414|Dixon Range beds|44139|5|Briefly described|p284, 285 Fig. 3-69|||Strongly deformed sandstone, siltstone, shale, conglomerate. Correlated with Bloods Range beds.| | ||||10-SEP-12
29414|Dixon Range beds|61154|6|Mentioned|p17|||May correlate with Tjauwata Group rocks.||||||
29414|Dixon Range beds|63562|6|Mentioned|p341|||Of Amadeus Basin. Part of the initial Basin fill.||Tjauwata Group.||||
29414|Dixon Range beds|64580|4|Described|map legend||Mesoproterozoic|Sandstone, siltstone, and conglomerate.||||||15-DEC-08
29414|Dixon Range beds|65102|6|Mentioned|p363, Figure 4-38|Mesoproterozoic|Mesoproterozoic|See also Amadeus Basin section p338 where shown as Arunta Complex?||||||25-MAR-15
29414|Dixon Range beds|65256|6|Mentioned|p40|||Previously correlated with Bloods Range Formation.||||||
29414|Dixon Range beds|67856|6|Mentioned|p337, p338, p339 fig 4-31|||Probably Middle Proterozoic.||||||
29414|Dixon Range beds|69606|5|Briefly described|p4 fig 2|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.||Tjauwata Group|||Sandstone.|
29414|Dixon Range beds|70839|5|Briefly described|p329-334,336,345|Mesoproterozoic|Mesoproterozoic|Of Amadeus Basin.  Exposed as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Detrital zircon age spectrum dominated by c. 1.22 and 1.1 Ga (derived from Pitjantjatjara Supersuite; Musgrave orogeny), with older 1.8-1.5 Ga component (maxima at 1.8, 1.77, 1.58, 1.5 Ga), and minor c. 1.04 Ga (Warakurna Supersuite) contribution.|Max dep age: 1029+\-17 Ma (207Pb/206Pb)|Unit of Tjauwata Group.||Correlable with Tjauwata Group.||
29414|Dixon Range beds|71088|6|Mentioned|p6-p8, p17|||Musgrave Province.||Tjauwata Group||||
29414|Dixon Range beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, shale, arkose|
29414|Dixon Range beds|71268|5|Briefly described|1m_geologyp12_lut.csv|||Sample GSWA 199408 (quartz sandstone) yielded a weighted mean 207Pb/206Pb age of 1147+\-13 Ma, interpreted as maximum depositional age of sandstone.||||Equivalent to upper Tjauwata Group or Bloods Range Formation.|Quartz sandstone, siltstone, shale, arkose, feldspathic sandstone and fine conglomerate with quartz-mica schist in places|
74728|Djilliri Limestone|64580|6|Mentioned|map legend|||Of Ningbing Group.||||||15-DEC-08
74728|Djilliri Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Late Devonian|||Ningbing Group||||
74728|Djilliri Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
74728|Djilliri Limestone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Ningbing Group.||||
40080|Dockerell Formation|6876|6|Mentioned|p100 Fig.5.|Paleogene|Paleogene|||||||
40080|Dockerell Formation|24205|6|Mentioned|p250 Fig. 6|||||||||
40080|Dockerell Formation|67970|5|Briefly described|p25 Fig.4.|Thanetian|Selandian|Exmouth Plateau.||||Overlies Lambert Formation.||
28508|Domal Rhyolite""|36551|6|Mentioned|p65|||||||||
74054|Dombey Formation, Lower|13242|3|Fully described|p217 Fig. 4, p220|Late Permian|Late Permian|Informal but  stated to be "defined" in text - see Dombey Formation. Unconformably overlies Cape Hay Formation. Geological Province: Bonaparte Basin. Dominantly a limestone unit (detailed lithology included). See also p226 Fig. 8.||||||07-FEB-11
74055|Dombey Formation, Upper|13242|3|Fully described|p217 Fig. 4, p221|Late Permian|Late Permian|Informal but  stated to be "defined" in text  - see Dombey Formation. Geological Prov: Bonaparte Basin. Dominantly a carbonate unit with basal marly section passing down into shale and sandstone (detailed lithology included). See also p226 Fig. 8.||||||07-FEB-11
77466|Dombey Limestone|67370|6|Mentioned|p313.|Late Permian|Late Permian|Bonaparte Basin. At Fishburn-1 well, this unit is absent because of erosion.||||Is overlain unconformably by Penguin Formation.||
74056|Dombey carbonates|13242|6|Mentioned|p221|Late Permian|Late Permian|Informal name - referring to Upper Dombey Formation.||||||07-FEB-11
80527|Dombey limestone, lower|71623|6|Mentioned|p345 fig 2, p347 fig 5, p352||Wuchiapingian|Bonaparte Basin.|||||Limestone.|
80528|Dombey limestone, upper|71623|6|Mentioned|p355, p345 fig 2,  p347 fig 5, p352||Wuchiapingian|Bonaparte Basin.|||||Limestone.|
76880|Dongara Formation|61546|6|Mentioned|p386.|||||||||
28509|Dongara Sandstone Member|23279|6|Mentioned|p17|||Present name: Dongara Sandstone.||||||
28509|Dongara Sandstone Member|29693|6|Mentioned|Fig.7|||||||||
28509|Dongara Sandstone Member|31910|4|Described|p19|||||||||
28509|Dongara Sandstone Member|32642|6|Mentioned|p74|||Oil production||||||
28509|Dongara Sandstone Member|36266|5|Briefly described|p150|Triassic|Triassic|Of Kockatea Shale. Lower triassic in age. Geological Province: Perth Basin.||||||31-MAR-08
28509|Dongara Sandstone Member|36293|6|Mentioned|p123|||||||||
28509|Dongara Sandstone Member|37577|6|Mentioned|p77|||||||||
28509|Dongara Sandstone Member|38484|6|Mentioned|p6|||||||||
28509|Dongara Sandstone Member|38655|6|Mentioned|p6|||||||||
28509|Dongara Sandstone Member|41195|4|Described|p322|||||||||
28509|Dongara Sandstone Member|43495|6|Mentioned|13|||||||||
28509|Dongara Sandstone Member|44144|5|Briefly described|p507 Tb.4-21, p513|Early Triassic|Early Triassic|Shoreline deposit.||Kockatea Shale (base of).|||Well-sorted orthoquartzite.|
28509|Dongara Sandstone Member|70097|6|Mentioned|p20 Fig.4|||Shown once as Wagina Formation (Dongara Sandstone Member) in North Perth Summary column (Fig.4). [possible accidental use of former names?] Elsewhere in paper, Wagina Sandstone (including in the same column as Wagina Formation in Fig.4) and Dongara Sandstone are used.||||||
83477|Dongarra Sandstone|73484|6|Mentioned|p476 Fig.3|Lopingian|Guadalupian|Perth Basin. Shallow marine. Abbreviated as Dongarra Sst.||||||
24251|Doolgunna Arkose|35975|4|Described|p100|||||||||
24251|Doolgunna Arkose|38994|5|Briefly described|p30|||||||||22-DEC-09
24251|Doolgunna Arkose|40297|6|Mentioned|p109|||||||||
24251|Doolgunna Arkose|40989|4|Described|p16|||||||||
24251|Doolgunna Arkose|49896|5|Briefly described|p2 Tb. 1|||||||||
24251|Doolgunna Arkose|62289|6|Mentioned|p12|Palaeoproterozoic|Palaeoproterozoic|Gee (1979). Superseded by Doolgunna Formation (Occhipinti et al., 1997).||||||
24251|Doolgunna Arkose|64384|6|Mentioned|p82|||Probably misspelt - see Doolgunna Formation.||||||07-FEB-11
24251|Doolgunna Arkose|65419|5|Briefly described|p5, p25.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979) and Elias et al. (1982); revised as Doolgunna Formation by Gee (1987) after recognising its heterolithic nature; further revised in this study. The northern part of this unit, as shown by Gee (1987), is now included in the Peak Hill Schist.||||||
24251|Doolgunna Arkose|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. Zero to 5km thick arkose-basalt-greywacke rift facies.||Glengarry Group||||
41226|Doolgunna-Thaduna Formation|50226|5|Briefly described|p421 Fig. 4|||Informal grouping of two units, Doolgunna Formation and the Thaduna Formation, of the Mooloogool Group.  Geological Province: Yerrida Basin.||||||24-JUN-04
28209|Dora Shale|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
28209|Dora Shale|35225|6|Mentioned|p9|||||||||
28209|Dora Shale|35711|4|Described|p24|||See also Table 3, stratigraphy||||||
28209|Dora Shale|35969|6|Mentioned|Fig.10|||||||||
28209|Dora Shale|35983|6|Mentioned|Table 28|||||||||
28209|Dora Shale|36890|3|Fully described|p343|||||||||
28209|Dora Shale|43173|6|Mentioned|54||Early Permian|||||||
28209|Dora Shale|44994|6|Mentioned|Fig.7|||Perm. Correlation.||||||
28209|Dora Shale|44998|2|Defined|86|Kungurian|Artinskian|Overlain by Triwhite Sandstone. Kungurian-Artinskian. On many pages. p.67,70,80,103-4,231,242.||||||
28209|Dora Shale|45153|2|Defined|App.4-69|Artinskian|Artinskian|||||||
28209|Dora Shale|48826|14|Not recorded|Tb.III|||Correlates with Noonkanbah Formation.||||||
28209|Dora Shale|66949|5|Briefly described|p13, p23, p26, p51 Appx.2, p59 Appx.3|||See also p74-75,78,82-83 Appx.5. Superseded: regarded as a synonym of Noonkanbah Formation. Type section detailed. About 12m thick. Available core detailed. Named [?informally] as Dora Member (of Grant Formation) by WAPET during revision of Parda 1 well completion report.||Formerly part of Grant Group.||Equivalent to Noonkanbah Formation.|Mudstone, minor sandstone.|
31935|Dora shale|43876|14|Not recorded|p573||Artinskian|||||||
81763|Dougall Suite|67323|5|Briefly described|p29|||Emplaced in an island arc setting (Tickalara arc).|~1850 Ma.||||Tonalite, trondhjemite.|
78627|Dougalls Granitoid Suite""|66845|6|Mentioned|p538|||Of Ogasawara (1988). See Dougalls suite.||||||
72893|Dougalls Granitoid suite|60724|5|Briefly described|p11, p14|||Informal name. See also Dougalls Tonalite. Of the Tickalara Metamorphics. Recrystallised, foliated, tonalite-rich granitoid.||||||
33973|Dougalls suite|22547|6|Mentioned|p13|||Probably mispelt||||||
33973|Dougalls suite|22754|5|Briefly described|p3, p6|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Age c. 1850 Ma||||||07-NOV-08
33973|Dougalls suite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|||||||07-FEB-07
33973|Dougalls suite|23751|6|Mentioned|p12|||Informal.||||||
33973|Dougalls suite|66845|4|Described|p535, p538, p539 Tb.1, p540-1, p543-4|Paleoproterozoic|Paleoproterozoic|Intrudes northern half of Central zone of Lamboo Complex at c. 1850 Ma. ?Interrelated with Tickalara Metamorphics. See also Dougalls Tonalite and "Dougalls Granitoid Suite"|||Dougalls Tonalite||sheets of mesocratic tonalite and quartz diorite, and leucocratic tonalite and minor trondhjemite, and gabbro|
33973|Dougalls suite|66846|4|Described|p547-554, p555-559 Fig.1, p549 Fig.2|Orosirian|Orosirian|In Central zone of Lamboo Complex. Not part of Bow River batholith. Geochemistry and variability discussed. Composition of this suite is atypical for Paleoproterozoic granites of northern Australia. Appears to be derived from partial melting of crustal rocks of mafic volcanics and turbiditic compositions. Neodymium isotopes rule out the similar Tickalara Metamorphics as a source. See also: many of the figures. Rare earth element abundances given on p551 Tb. 2.|c.1850 Ma||||Includes tonalite and trondhjemite sheets.|
33973|Dougalls suite|72437|5|Briefly described|p6, p45-47|Palaeoproterozoic|Palaeoproterozoic|The Dougalls Granitoid Suite of Ogasawara 1988.|c. 1850 Ma||||Recrystallised tonalite, minor quartz diorite, trondhjemite and gabbro.|
69905|Dresser Chert|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Probably an informal reference to a cherty layer in the Dresser Formation. Geological Province: North Pole Dome of the Pilbara Craton.||||||09-OCT-15
69905|Dresser Chert|62979|5|Briefly described|p212 Fig. 1|Archean|Archean|Cherty layer within the Dresser Formation - probably not intended as a formal name. Geological Province: Pilbara Craton.||||||07-FEB-11
69906|Dresser Formation, upper|61257|6|Mentioned|p355|Archean|Archean|Informal - see Dresser Formation.||||||07-NOV-08
38619|Dresser barite|23784|6|Mentioned|p6|||||||||
79812|Dromedary Bore Tonalite|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
79812|Dromedary Bore Tonalite|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Bunnawarra Suite|||Tonalite.|
79812|Dromedary Bore Tonalite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
40449|Duck Creek Dolomite, middle|24602|6|Mentioned|p861|||Geological Province: Ashburton Fold Belt. Informal - see Duck Creek Dolomite.||||||
40450|Duck Creek Dolomite, upper|24602|6|Mentioned|p861|||Geological Province: Ashburton Fold Belt. Informal - see Duck Creek Dolomite.||||||
41227|Duck Creek dolomite|50226|5|Briefly described|p415, p416|Paleoproterozoic|Paleoproterozoic|Informal - see Duck Creek Dolomite.  Of the Upper part of the Wyloo Group.  Age: ~2.0Ga (Lindsay and Brasier, 2002).||||||07-NOV-08
24932|Duck Pond slate|33513|6|Mentioned|p32|||Stratigraphy||||||
24932|Duck Pond slate|33515|6|Mentioned|p35|||||||||
28162|Dudawa Beds|24160|6|Mentioned|p27 Tb. 14|||Correlated to part of Coomberdale Subgroup. [Database says it has been replaced by Jingenia Dolomite].||||||
28162|Dudawa Beds|24410|6|Mentioned|p142 Tb. 60|Proterozoic|Proterozoic|?Together with Coomberdale Chert, superseded by Jingemia Dolomite of the Coomberdale Subgroup (Moora Group). ||||||
28162|Dudawa Beds|36293|2|Defined|p76|Neoproterozoic|Mesoproterozoic|Middle or Late Proterozoic.||||||
28162|Dudawa Beds|36551|6|Mentioned|p141|||||||||
28162|Dudawa Beds|36872|3|Fully described|p74|||||||||
28162|Dudawa Beds|37460|5|Briefly described|p178|||||||||
28162|Dudawa Beds|38988|6|Mentioned|p13|||||||||
28162|Dudawa Beds|40089|6|Mentioned|p12|||||||||
28162|Dudawa Beds|40347|6|Mentioned|p14|||||||||
28162|Dudawa Beds|41341|6|Mentioned|p8|||||||||
39435|Duedin Group|22754|5|Briefly described|p5 Tb. 1|Neoproterozoic|Neoproterozoic|Misspelt - see Duerdin Group.  Geological Province: Wolfe Creek Basin.||||||
41592|Duerdin group|22496|6|Mentioned|p12|Neoproterozoic|Neoproterozoic|Informal - see Duerdin Group.||||||
24934|Duffer volcanics|35142|6|Mentioned|p423|||||||||
38138|Dugal Gneiss|23569|5|Briefly described|p3|Archean|Archean|Misspelt - see Dugel Gneiss.   Age: 3400Ma||||||07-NOV-08
72638|Dugel leucogneiss|62842|6|Mentioned|p217|Archean|Archean|Age: ca 3300Ma (zircon, Kinny et al., 1988)||||||07-NOV-08
80317|Duke Monzonite|67202|5|Briefly described|p184|Tonian|Tonian|Yeneena Basin. Unclear if this is meant to be a formal name.|835 +/- 4 Ma (Maidment, pers. Comm.).|||Correlates with Gairdner Dyke Swarm.||31-JAN-18
24935|Dumbardo Siltstone Member|37920|5|Briefly described|p453|||||||||
28517|Dumbardo Siltstone""|33594|6|Mentioned|p37|||||||||
28517|Dumbardo Siltstone""|37920|6|Mentioned|p453|||||||||
32614|Dundas Dyke Suite|44316|14|Not recorded|map legend||Archean|||||||07-NOV-08
32614|Dundas Dyke Suite|46311|14|Not recorded|p.11,15||Paleoproterozoic|Opposite p.6; map. ?L.Proterozoic.||||||07-NOV-08
32614|Dundas Dyke Suite|46316|14|Not recorded|p.11||Paleoproterozoic|Replaced by Widgiemooltha Dyke Suite. L. Proterozoic (H51-14).||||||07-NOV-08
73779|Dundas Granite|50542|6|Mentioned|p135|Archean|Archean|||||||07-FEB-11
37930|Dunnsville Granite|24305|5|Briefly described|p927|||||||||
40170|Dunsborough Suite|24595|5|Briefly described|p588 Tb. 1|||Of Kay (1958).  Part of the Leeuwin Complex.  Later referred to as Hamelin Granite by Myers (1994).  Geological Province: Leeuwin Block.||||||
35981|Dupuy Massive Sands|23379|5|Briefly described|p160 Fig.2;p162|Tithonian|Kimmeridgian|Informal name for sandstones within the Dupuy Formation. of Barrow Sub-basin, Carnarvon Basin.||||||
28521|Dupuy Member|24059|4|Described|p131|||Of Dingo Claystone. Max. thickness: 1240m.  Geological Province: Barrow Sub-basin.||||||
28521|Dupuy Member|30304|3|Fully described|p51|||Tithonian age. Member of Dingo Claystone||||||
28521|Dupuy Member|31561|4|Described|p34|||See also P38. Late Jurassic.||||||
28521|Dupuy Member|33386|6|Mentioned|Fig.7|||||||||
28521|Dupuy Member|33453|5|Briefly described|p71|||Mid.Jurrissic. Near shore marine.||||||
28521|Dupuy Member|34840|6|Mentioned|p66|||||||||
28521|Dupuy Member|34846|6|Mentioned|Fig.3|||||||||
28521|Dupuy Member|35282|6|Mentioned|p23|||||||||
28521|Dupuy Member|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
28521|Dupuy Member|37320|6|Mentioned|p235|||||||||
28521|Dupuy Member|39427|6|Mentioned|p18|||||||||
28521|Dupuy Member|39486|6|Mentioned|p2092|||||||||
28521|Dupuy Member|41271|6|Mentioned|p128|||||||||
28521|Dupuy Member|41439|4|Described|p116|||||||||
34474|Durack Range kimberlites|22754|6|Mentioned|p22|||A Late Proterozoic age of c.800 Ma is suggested by other similar occurrences in north Kimberley.||||||
41044|Durang granodiorite|24196|5|Briefly described|p73|Archean|Archean|Informal name Age: 2672 +/- 2 Ma. Geological Province: Merolia Domain, Yilgarn Craton.||||||07-NOV-08
74718|Earaheady Group|64580|6|Mentioned|map legend|||Misspelling of Earaheedy Group.||||||15-DEC-08
27144|Earaheedy Group|7161|6|Mentioned|p100, p101|||||||||
27144|Earaheedy Group|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Shallow-marine transgression.||Includes the Tooloo and Miningarra Subgroups.||||
27144|Earaheedy Group|12099|5|Briefly described|p676-7, 681, 684, 685-6, Figs.1, 2,6, 8|Paleoproterozoic|Paleoproterozoic|Contains Pb mineralisation.|||Includes Mount Leake and Yelma Formations.|Unconformably overlies Yerrida Group.||04-MAR-13
27144|Earaheedy Group|22478|6|Mentioned|p23||Paleoproterozoic|Nabberu Basin||||||07-NOV-08
27144|Earaheedy Group|22491|5|Briefly described|p 9||Paleoproterozoic|Yilgarn Craton||||||07-NOV-08
27144|Earaheedy Group|22493|6|Mentioned|p100|||||||||
27144|Earaheedy Group|22501|5|Briefly described|p117|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|22716|5|Briefly described|table4, p229|Paleoproterozoic|Paleoproterozoic|Deposited in the Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Savory Sub-basin.||||||19-SEP-06
27144|Earaheedy Group|22896|6|Mentioned|104|||Geol province Earaheedy Basin||||||
27144|Earaheedy Group|22903|6|Mentioned|63 fig 1|||||||||
27144|Earaheedy Group|22940|6|Mentioned|Fig.1 p3|||||||||
27144|Earaheedy Group|23133|5|Briefly described|p293|||||||||
27144|Earaheedy Group|23151|6|Mentioned|p64 Fig.1|||||||||
27144|Earaheedy Group|23152|5|Briefly described|p71|||||||||
27144|Earaheedy Group|23253|6|Mentioned|p2|||Geological Province:  Earaheedy Basin.||||||12-SEP-05
27144|Earaheedy Group|23529|4|Described|p7|Paleoproterozoic|Paleoproterozoic|Geological Province:  Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||||||07-NOV-08
27144|Earaheedy Group|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||||||07-NOV-08
27144|Earaheedy Group|23580|5|Briefly described|Map legend||Proterozoic|In the Earaheedy Basin||||||
27144|Earaheedy Group|23581|5|Briefly described|Map legend||Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|23587|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Age: c. 1850 -1800 Ma. Geological Province: Earaheedy Basin.||||||17-NOV-08
27144|Earaheedy Group|23588|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|23589|4|Described|p20|Proterozoic|Proterozoic|Age: 1700 Ma (K-Ar (glauconite)) of Yelma Formation. Overlying unit Bangemall Group. Underlying unit Yerrida Group. Geological Province: Earaheedy Basin.||||||19-SEP-06
27144|Earaheedy Group|23593|5|Briefly described|p6|||Underlying unit Yerrida Group.||||||
27144|Earaheedy Group|23597|4|Described|p11|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|23600|5|Briefly described|p16|||Underlying unit Yerrida Group. Geological Province: Earaheedy Basin.||||||
27144|Earaheedy Group|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1.  Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|23744|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Age: 1900-1800 Ma. See also page 2 Fig 1. Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|23747|5|Briefly described|p16|||||||||
27144|Earaheedy Group|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Earaheedy Basin.||||||28-JUL-08
27144|Earaheedy Group|23749|5|Briefly described|p14|Proterozoic|Proterozoic|Geological Province: Earaheedy Basin.||||||
27144|Earaheedy Group|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Earaheedy Basin.||||||
27144|Earaheedy Group|23759|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|23760|6|Mentioned|p5|||||||||
27144|Earaheedy Group|23865|6|Mentioned|p170 Fig.1|||Geological Province: Yilgarn Craton.||||||
27144|Earaheedy Group|23890|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24017|3|Fully described|p11|Paleoproterozoic|Paleoproterozoic|Thickness: 5000m. Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24021|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24028|5|Briefly described|p288 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|24135|5|Briefly described|p3 Fig.1|Proterozoic|Proterozoic|||||||
27144|Earaheedy Group|24183|5|Briefly described|p2 Fig.1, p20|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by the Collier Group.||||||
27144|Earaheedy Group|24535|5|Briefly described|p4, 5, 10, 15, 23|||Intruded by Prenti Dolerite.||||||26-NOV-13
27144|Earaheedy Group|24578|5|Briefly described|p775|Paleoproterozoic|Paleoproterozoic|Age: <1.85 Ga. Geological Province: Earaheedy Basin. Maximum Thickness: ~ 5km.||||||07-NOV-08
27144|Earaheedy Group|30010|6|Mentioned|p43|||||||||
27144|Earaheedy Group|31217|2|Defined|p40|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|35949|6|Mentioned|Fig.8|||||||||
27144|Earaheedy Group|35975|6|Mentioned|p104|||||||||
27144|Earaheedy Group|36551|6|Mentioned|Table 29|||||||||
27144|Earaheedy Group|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|37299|6|Mentioned|Fig.1|||||||||
27144|Earaheedy Group|37300|6|Mentioned|p81|||||||||
27144|Earaheedy Group|37460|6|Mentioned|p143|||||||||
27144|Earaheedy Group|38243|6|Mentioned|Fig.2|||||||||
27144|Earaheedy Group|38515|4|Described|p9|||||||||
27144|Earaheedy Group|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|38978|6|Mentioned|p146|||||||||
27144|Earaheedy Group|38988|6|Mentioned|p8|||||||||
27144|Earaheedy Group|38994|6|Mentioned|p34|||||||||
27144|Earaheedy Group|39894|6|Mentioned|p48|||||||||
27144|Earaheedy Group|40089|6|Mentioned|p4|||||||||
27144|Earaheedy Group|40103|6|Mentioned|p185|||||||||
27144|Earaheedy Group|40105|6|Mentioned|Fig.3|||||||||
27144|Earaheedy Group|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|40355|4|Described|p5|||||||||
27144|Earaheedy Group|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|40937|6|Mentioned|p5|||||||||
27144|Earaheedy Group|40938|4|Described|p13|||Mention p3.||||||19-SEP-06
27144|Earaheedy Group|40939|5|Briefly described|p108|||||||||
27144|Earaheedy Group|40989|4|Described|p28|||Mention p16.||||||19-SEP-06
27144|Earaheedy Group|41846|6|Mentioned|p102|||||||||
27144|Earaheedy Group|41997|6|Mentioned|p73|||||||||
27144|Earaheedy Group|42191|6|Mentioned|p446|||||||||
27144|Earaheedy Group|42548|5|Briefly described|p52|||||||||
27144|Earaheedy Group|42708|5|Briefly described|Plate 1|Proterozoic||||||||
27144|Earaheedy Group|42730|5|Briefly described|p15|||||||||
27144|Earaheedy Group|43069|5|Briefly described|p19|||see also Fig.1||||||
27144|Earaheedy Group|43238|5|Briefly described|p7|||||||||
27144|Earaheedy Group|43561|6|Mentioned|p1436|||||||||
27144|Earaheedy Group|43595|5|Briefly described|p75,219,343,344||Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|43652|6|Mentioned|p381||Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||18-MAY-04
27144|Earaheedy Group|44111|6|Mentioned|p.56 Fig. 1|||||||||
27144|Earaheedy Group|44142|5|Briefly described|p315 Tb.4-4, p321, p324|||Of Nabberu Basin.|||Includes Frere Formation.|Is overlain unconformably by Coonabildie Formation and Collier Subgroup (also faulted against the latter).||13-MAR-18
27144|Earaheedy Group|44149|6|Mentioned|p81-83 Tb.2-8|||||||||
27144|Earaheedy Group|44830|5|Briefly described|Map Legend||Proterozoic|||||||
27144|Earaheedy Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27144|Earaheedy Group|49893|5|Briefly described|p2 Fig.1, p5|||Overlies the Yerrida Group.||||||
27144|Earaheedy Group|49895|6|Mentioned|p5|||||||||
27144|Earaheedy Group|49896|5|Briefly described|p4 Fig. 1, p6|||Lower formations of the group have been correlated with Padbury Group. ||||||
27144|Earaheedy Group|50188|5|Briefly described|p2, p3, Fig. 1|||Geological Province: Stanley Fold Belt/ Earaheedy Basin. Divided into Tooloo and Miningarra Subgroups.||||||16-JUL-08
27144|Earaheedy Group|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Tooloo and Miningarra Subgroups.  Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|50222|4|Described|p320 Fig. 3, p327, p336|Paleoproterozoic|Paleoproterozoic|Subdivided into 2 subgroups: Tooloo and Miningarra Subgroups. Shallow marine clastic and chemical sedimentary rocks. Overlies the Mooloogool Group.  Age: <1.84Ga.  Max. thickness: 5km.  Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|50223|5|Briefly described|p344, p346|Paleoproterozoic|Paleoproterozoic|Subdivided into Miningarra and Tooloo Subgroups.  Max. thickness: 5km.  Geological Province:  Earaheedy Basin/ Stanley Fold Belt.||||||07-NOV-08
27144|Earaheedy Group|50224|5|Briefly described|p368, p369 Fig. 1|Paleoproterozoic|Paleoproterozoic|Divided into Tooloo and Minningarra Subgroups.  Age: <1990+/-6Ma. Geological Province: Earaheedy Basin.||||||07-FEB-11
27144|Earaheedy Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
27144|Earaheedy Group|50226|5|Briefly described|p420, p423|Paleoproterozoic|Paleoproterozoic|Comprises the Miningarra and Tooloo Subgroups.  Unconformably overlies Windplain and Mooloogool groups.  Max. thickness: 5km.  Intruded by 1.0Ga sills and dykes. Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.  Includes: Miningarra Subgroup, Tooloo Subgroup.||||||07-NOV-08
27144|Earaheedy Group|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes the Tooloo and Miningarra Subgroups.  Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin. Metasandstone, metasiltstone and phyllite.||||||07-NOV-08
27144|Earaheedy Group|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-NOV-08
27144|Earaheedy Group|61269|6|Mentioned|p86 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27144|Earaheedy Group|61271|6|Mentioned|p106|Proterozoic|Proterozoic|||||||
27144|Earaheedy Group|61564|5|Briefly described|p588, p590 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes the Tooloo and Miningarra Subgroups. Age: <1.8Ga. Geological Province: Earaheedy Basin. ||||||07-NOV-08
27144|Earaheedy Group|61732|5|Briefly described|p26|Mesoproterozoic|Mesoproterozoic|Includes the Frere Formation.||||||07-FEB-11
27144|Earaheedy Group|62289|4|Described|plate 1, p1-3, p7 Fig. 3, p29, p32|Palaeoproterozoic|Palaeoproterozoic|Includes Mount Leake and Yelma Formations; Geol. Prov: outliers of Earaheedy Basin, which in part overlie the Yerrida Basin.||||||
27144|Earaheedy Group|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Earaheedy Basin.|||Includes Yelma Formation.|||14-APR-11
27144|Earaheedy Group|62453|6|Mentioned|p9|||||||||
27144|Earaheedy Group|63866|4|Described|p152, p165-p166|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. Late Paleoproterozoic. Shallow water shelf deposits.|||Includes the Miningara Subgroup and the Tooloo Subgroup.|Unconformably overlain by the Collier Group. Equivalent to the Mount Leake Formation. Unconformably overlies the Mooloogool Group. Unconformably overlies the Yerrida Group.||29-MAR-18
27144|Earaheedy Group|64161|4|Described|p581, p587, p591 Fig.11, p592-595|Statherian|Orosirian|Max depositional age of ~1843 Ma, but some ~1800 Ma grains identified. Possible equivalent of Woodline Formation.|||Includes Yelma and Chiall Formations.||Coastal to shallow-marine ~5km thick succession of siliciclastic and chemical sediments.|21-MAR-12
27144|Earaheedy Group|64283|5|Briefly described|p53|Paleoproterozoic|Paleoproterozoic|Of the Capricorn Orogen. Age: c.1800Ma (Jones et al 2000).||||||07-FEB-11
27144|Earaheedy Group|64284|5|Briefly described|p57, p58 Fig. 1, p61|Paleoproterozoic|Paleoproterozoic|Stromatolite taxa indicate age to be in 1.9Ga-1.8Ga range; but isotopic ages for sed.rocks + mineralisation cluster around 1800-1700Ma. Thickness: 5km. Geol.prov:Earaheedy Basin. Subdivided into lower Tooloo and upper Minningarra Subgroups||||||07-FEB-11
27144|Earaheedy Group|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin.||||||07-FEB-11
27144|Earaheedy Group|64655|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Tooloo Subgroup.||||||
27144|Earaheedy Group|64724|6|Mentioned|p45 Fig.5|Statherian|Statherian|Deposited during the Leichhardt Extension (1800-1750 Ma). ||||||
27144|Earaheedy Group|64725|5|Briefly described|p59, p73.|||Capricorn Orogen; Yerrida Basin. A 5 km thick succession of shallow-marine clastic and chemical sedimentary rocks. Hosts the Magellan Pb deposit.|||Includes Tooloo and Miningarra Subgroups.|||02-APR-12
27144|Earaheedy Group|64728|6|Mentioned|p94 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||Is unconformably overlain by Bangemall Supergroup.||
27144|Earaheedy Group|64748|5|Briefly described|p276|Statherian|Orosirian|In the Earaheedy Basin; younger than 1.84 Ga; probably older than 1.79-1.76Ga; Broadly coeval with the Kimberley Group||||||
27144|Earaheedy Group|64772|5|Briefly described|p9-12, Plate 1|Paleoproterozoic|Paleoproterozoic|Includes 6 named formations and Miningarra and Tooloo Subgroups, and basal undivided units of sandstone, dolomite, siltstone, and shale; minor conglomerate and limestone. Age range: <2027Ma to <1808Ma. Geological province: Earaheedy Basin. On Plate 1, Chiall Formation shown within Tooloo Subgroup, and Miningarra Subgroup not shown. Shoemaker impact structure affects rocks of the Earaheedy Group (Yelma, Frere, and Chiall Formations).p5, p8, p17, p20-21 Fig.10, p25 Fig.11, p25 Fig.12, p26 Fig.14, p43 Fig.28, p44, p51, p69 App.4,||||Overlies Bardsley Formation||25-NOV-13
27144|Earaheedy Group|65102|6|Mentioned|p363, Figure 4-38|Mesoproterozoic|Paleoproterozoic|Nabberu Basin.||||||
27144|Earaheedy Group|65264|5|Briefly described|p8 Fig.3, p27, p44 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes the Tooloo (lower) and Miningarra (upper) Subgroups. Geological province: Earaheedy Basin. Comprises clastic and chemical sedimentary rocks of shallow-marine environments. See also p44 Appdx. 1||||||07-FEB-11
27144|Earaheedy Group|65404|6|Mentioned|p245 Fig.1|||||||||
27144|Earaheedy Group|65408|6|Mentioned|p82, p84 Fig.1.|||||||Unconformably overlies Yerrida Group.||
27144|Earaheedy Group|65411|6|Mentioned|p89 Fig.1.|||||||||
27144|Earaheedy Group|65412|6|Mentioned|p97 Fig.1.|||||||||
27144|Earaheedy Group|65419|1|Redefined|p2, p4 Fig.1, p6, p13, p19, pp46-50.|Paleoproterozoic|Paleoproterozoic|Of Hall et al. (1977) and Hall and Goode (1978); revised by Bunting (1986); and in this study to include outliers of the Yelma Formation on Peak Hill and Glengarry 1:250 000 sheets, and to incorporate the Mount Leake Formation. No type section; type area is in the Earaheedy Basin. Thickness is c.6300 m; in the area of this study, up to tens of metres only. Age from detrital zircons. The Group is younger than the Padbury Group (1.9 Ga) and older than the Bangemall Group (1.65 Ga).|1785 +/- 11 Ma (Nelson, 1997) from p6.||Includes Tooloo and Miningarra Subgroups and Mount Leake, Frere and Yelma Formations.|Unconformably overlies Yerrida and Bryah Groups.|Arenite and argillite siliciclastic rocks, chert, carbonate, and stromatolitic carbonate.|15-NOV-13
27144|Earaheedy Group|65472|5|Briefly described|p1, p2, p3 Fig.2, p4, p5 Fig. 4, p6|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. 5 km thick succession of shallow marine clastic and chemical sedimentary rocks. |||Tooloo Subgroup at base, Miningarra Subgroup|Unconformably overlies Yilgarn Craton, Mooloogool Group, and, outliers unconformably overlie Juderina Formation (Windplain Group).||
27144|Earaheedy Group|65487|6|Mentioned|p24|Paleoproterozoic|Paleoproterozoic|Occurs on the NE margin of the Yilgarn Craton. Similar detrital zircon age to the Woodline Formation which has a maximum depositional age of 1737 +/- 28 Ma.||||||10-FEB-14
27144|Earaheedy Group|65506|5|Briefly described|p986-994, p996-999|Mesoproterozoic|Mesoproterozoic|5000m thick succession of shallow-marine siliciclastic and chemical sedimentary rocks. Contains dolerite sills (geochemistry detailed). Overlain by Bangemall Supergroup. Maximum depositional age of 1808 +/- 36 Ma. Mis-spelt as Earaheady p987.||||||
27144|Earaheedy Group|65692|6|Mentioned|p9, p55-56|||Earaheedy Basin.|||Tooloo and Miningarra Subgroups.|||
27144|Earaheedy Group|65899|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. Includes Yelma and Frere Formations.||||||
27144|Earaheedy Group|65913|4|Described|p2 Fig.1, pp4-5, pp19-21. |Paleoproterozoic|Paleoproterozoic|Flat-lying deposits form mesas over the Maraloou Formation plains in the southwestern area of the map. Minimum age limit of 1630 Ma (Bunting et al. 1980) comes from a syenite intrusive in the Teague Ring Structure which post-dates this unit. Depositional age probably 2.0 - 1.9 Ma. Thickness to 60 m. A sample of ironstone capping rubbly stromatolitic dolomite had 1090 ppm Mo; the origin is possibly fault-related.|1785 +/- 11 Ma (zircon xenocryst) (Nelson 1997).||Includes Yelma Formation.|Unconformably overlies Yerrida Group.||
27144|Earaheedy Group|66115|6|Mentioned|p136|||||||||
27144|Earaheedy Group|66427|5|Briefly described|p39, p42-44, p46-51, p62, p69-74|||Earaheedy Basin, the easternmost end of the Capricorn Orogen. Contains stromatolites similar to taxa aged 1900-1800 Ma in Duck Creek Dolomite. Maximum and minimum ages not well constrained. Geochronology and likely sources of detrital zircons detailed.|||Includes the Tooloo and Miningarra Subgroups.|Intruded by dykes and sills of the Glenayle Dolerite and Prenti Dolerite. Conformably overlies the Mooloogool Group.|5-km thick succession of shallow marine clastic and chemical sedimentary rocks, with basal fluvial sandstone and conglomerate.|
27144|Earaheedy Group|67855|5|Briefly described|p203, p207-209, 204, 202, 205, 206,|Paleoproterozoic|Paleoproterozoic|Of Hall and others 1977). Eastern Nabberu Basin. Previously correlated with  Padbury Group, but this now in doubt.|~ 1.67 - 1.7 Ga.||Includes Tooloo and Minningarra Subgroups.|Unconformably overlies Glengarry Group.||
27144|Earaheedy Group|67888|6|Mentioned|p96|||||||||
27144|Earaheedy Group|68055|6|Mentioned|p76-77, 87-88|Proterozoic|Proterozoic|Earaheedy Basin. No robust dates for this unit.|||Tooloo, Miningarra Subgroups.|||
27144|Earaheedy Group|69080|6|Mentioned|p684|||Variably deformed low-grade metasedimentary rocks.||||||
27144|Earaheedy Group|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|||Earaheedy Basin|||Includes Tooloo Subgroup, Miningarra Subgroup|||
27144|Earaheedy Group|69313|6|Mentioned|p19, p21, p23, p24, p87, p88|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin, Capricorn Orogen. Deposited on the established passive margin, with a spreading centre to east-north east.|||Tooloo Subgroup, Minningarra Subgroup.|||
27144|Earaheedy Group|69595|6|Mentioned|p19|||Yilgarn Craton.||||Possible lateral equivalent of the Woodline Formation.||
27144|Earaheedy Group|70276|6|Mentioned|p783|Proterozoic|Proterozoic|Overlies and terminates the northern end of the Agnew-Wiluna greenstone belt.||||||
27144|Earaheedy Group|70804|5|Briefly described|p4, p6, p37-p38||||||Includes the Mount Leake Formation.|Unconformably overlies the Bryah Group.||
27144|Earaheedy Group|71042|6|Mentioned|p66 fig 2, p98|Paleoproterozoic|Paleoproterozoic|||||||28-MAY-19
27144|Earaheedy Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, arkose, siltstone|
27144|Earaheedy Group|71269|5|Briefly described|1m_geologyp12_lut.csv|||Of Edmund Basin. Events: Mulka Tectonic Event (570-570 Ma); Edmundian Orogeny (1026-954 Ma); Mutherbukin Tectonic Event (1321-1171 Ma). ||||||
27144|Earaheedy Group|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 100k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|||Includes Miningarra Subgroup, Tooloo Subgroup.|||
27144|Earaheedy Group|71310|6|Mentioned|p766|Proterozoic|Proterozoic|||||||
27144|Earaheedy Group|71484|6|Mentioned|p122,130|||Nomenclature proposed by Hall and Goode 1978 to describe stratigraphy in the eastern part of the Nabberu Basin, then revised to be entirely dominant in the Earaheedy Basin (Gee and Grey, 1993). Abandoned; obsolete. See Tooloo and Miningarra groups.|||Includes Tooloo and Miningarra subgroups.|||30-AUG-19
42478|Earaheedy group|50216|6|Mentioned|p208|||||||||14-JAN-05
42478|Earaheedy group|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|Sedimentary rocks.||||||07-FEB-11
80937|Early Merougil Group|72049|4|Described|p251, p254, p256|||Kalgooglie Terrane. See also p259-p260, p264, p266-p267, p269-p272.|c. 2670-2660 Ma||Includes the Merougil Sandstone, Killaloe Formation, Navajo Sandstone and Penny Dam Conglomerate.||Coarse-grained, quartz-rich rocks including massive quartz-rich sandstone.|
32612|East Gibraltar Granite|46311|14|Not recorded|p.10||Archean|||||||07-NOV-08
41045|East Leonora basalts|24196|6|Mentioned|p69 Fig.10|||Informal name - see also West Leonora basalts. Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||28-MAY-04
69861|East Pilbara granitoid complexes|60903|5|Briefly described|p833 Fig. 2|Archean|Archean|Age: 3.49-2.83Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
38590|Eastern Granite|23782|5|Briefly described|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
38590|Eastern Granite|23904|5|Briefly described|p26, p31|||Informal name.  Geological Province: Yilgarn Craton.||||||
38590|Eastern Granite|60667|5|Briefly described|p1125, p1126 Fig. 2|||Quartz-feldspar monzogranite.||||||
70569|Eastern Shoal sediment|61521|6|Mentioned|p39|||Informal name. Carbonate muddy sand.||||||
38592|Eastern Ultramafic|23782|6|Mentioned|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
38592|Eastern Ultramafic|60514|6|Mentioned|p94, p95, p96 Fig. 2|Archean|Archean|Geological Province: Yilgarn Craton. Contains accumulations of extreme olivine-cumulate rocks with olvine grainsizes up to 2.5 cm. Dips steeply to the west.||||||07-FEB-11
38592|Eastern Ultramafic|60628|4|Described|p87, 90|||Thick (>500m) coarse-grained cumulate rocks. Contains dacitic units. Dips steeply to the west. Overlain by Central Ultramafic. Local name.||||||
38592|Eastern Ultramafic|60629|5|Briefly described|p93-95|||Contains olivine-cumulate rocks (dunite and mesocumulate peridotite). Dips steeply to the west. Intrusive. Local name. Overlain by Central Ultramafic. See also Eastern Ultramafic unit.||||||
38589|Eastern Ultramafic Unit|23782|5|Briefly described|p46|||Informal name.  Geological Province: Yilgarn Craton.||||||
69190|Eastern Ultramafic unit|60628|6|Mentioned|p89 Fig.2|||Local name. See also Eastern Ultramafic.||||||13-JUN-05
69190|Eastern Ultramafic unit|60629|5|Briefly described|p93-95|||Dips steeply to the west. Local name. See also Eastern Ultramafic.||||||
69035|Eastmans Granite|44231|5|Briefly described|Map Legend|||Medium- to coarse-grained, leucocratic biotite syenogranite and monzogranite.||||||
74719|Eastmans intrusion|64580|6|Mentioned|map legend|||Included in undivided mafic-ultramafic intrusions; may have interlayered metasedimentary rocks. Different unit to  Eastman Granite?||||||
28524|Eaton formation|40367|6|Mentioned|Fig.4 p75 (caption)|||Informal - see Eaton Sand.||||||07-AUG-07
39269|Echuca Shoals|24207|4|Described|p212-213|Barremian|Valanginian|Abbreviated name for Echuca Shoals Formation.  Max. thickness: 50m.  Geological Province: Vulcan Sub-basin.||||||01-MAR-10
39269|Echuca Shoals|24234|6|Mentioned|p293 Fig.13|Early Cretaceous|Early Cretaceous|Abbreviation of Echuca Shoals Formation. Geological Province: Bonaparte Basin.||||||
39269|Echuca Shoals|50027|5|Briefly described|p10|Early Cretaceous|Early Cretaceous|Geological Province: Browse Basin.||||||
39269|Echuca Shoals|65078|6|Mentioned|p35|||Contain a clastic "basal transgressive sand" which indicates deltaics and general shallow marine geology.  Geological province: Vulcan Sub-basin.||||||30-APR-09
69383|Eclipse mafic-ultramafic unit|60980|5|Briefly described|p142 Fig.2, p145|||Informal name||||||27-JUN-05
81349|Eddy schist|70090|5|Briefly described|p447-448, 453|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton. [Also referred to as Eddy Suite on p458?]. Maximum depositional age: c.1629 Ma. Minimum depositional age: contrained by c. 1665 Ma granitic intrusion into Eddy schist. Detrital zircon Paleoproterozoic age components include c. 1783, 1745 and 1650 (major) Ma. Includes ca. 2645 Ma Archean component. Late Paleoproterozoic detrital age components suggest derivation from local Biranup Zone sources.|c. 1665 Ma|||||08-AUG-19
40185|Edel formation|23520|6|Mentioned|p3|||Informal reference by oil company to parts of the Tumblagooda Sandstone.||||||
70182|Edeowie glass|61560|6|Mentioned|p498|||Informal name. A glass field in central South Australia interpreted to have been caused by an impact - due to rare rock fragment inclusion contained planar microstructures. ||||||
32728|Edgar Range Beds""|44997|14|Not recorded|P.41|||||||||
32726|Edgar Range Group|44997|14|Not recorded|p.37|||||||||
67856|Edjudina-Laverton greenstones|60076|5|Briefly described|p14|Archean|Archean|Informal grouping of greenstones in the Edjudina terrane and Laverton Sub-province region.||||||07-NOV-08
40744|Edmund Group, lower|24183|6|Mentioned|p6|||||||||
40744|Edmund Group, lower|50225|6|Mentioned|p389, p390|||Informal - see Edmund Group. Significant modifications have been made to the units comprising this lower section, resulting in several redefinitions and abandonments of names. Coeval with lower McArthur Group (NT).||||||02-SEP-20
26264|Edmund Subgroup|22694|4|Described|p7|Proterozoic|Proterozoic|Bangemall Basin||||||
26264|Edmund Subgroup|22716|5|Briefly described|table4, p236|Statherian|Statherian|Age: 1640 Ma.||||||
26264|Edmund Subgroup|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
26264|Edmund Subgroup|22905|5|Briefly described|p52-53|Mesoproterozoic|Mesoproterozoic|Superseded by Edmund Group.||||||20-MAY-04
26264|Edmund Subgroup|22907|6|Mentioned|41|||Parent Bangemall Group||||||
26264|Edmund Subgroup|22940|4|Described|p20|Mesoproterozoic|Mesoproterozoic|of Bangemall Group.||||||
26264|Edmund Subgroup|23403|6|Mentioned|p4|||Now been given Group status - see Edmund Group.||||||
26264|Edmund Subgroup|23485|6|Mentioned|p30|||Superseded by Edmund Group.||||||
26264|Edmund Subgroup|23592|5|Briefly described|p9 Table 1|Paleoproterozoic|Paleoproterozoic|Age: c.1640 Ma. Geological Province: Bangemall Basin.||||||07-NOV-08
26264|Edmund Subgroup|23749|5|Briefly described|p14|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
26264|Edmund Subgroup|24183|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Superseded by the Edmund Group. Of the Bangemall Group.||||||
26264|Edmund Subgroup|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Superseded by Edmund Group. Overlain by Mucalana Subgroup.||||||
26264|Edmund Subgroup|40089|2|Defined|p17|Mesoproterozoic|Mesoproterozoic|||||||
26264|Edmund Subgroup|42013|5|Briefly described|Map Legend|Proterozoic||||||||
26264|Edmund Subgroup|42471|5|Briefly described|p19|||||||||
26264|Edmund Subgroup|43561|5|Briefly described|Fig.3,1434,1436,1438|||||||||
26264|Edmund Subgroup|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26264|Edmund Subgroup|44142|5|Briefly described|p309 Fig.4-13, p310 Tb.4-3, p311|||See also p312-314 Tb.4-4, p319-321, p324. Also includes Discovery Chert. Western half of Bangemall Basin. Interpreted as a transgressive (onto the Ashburton Fold Belt) and later regressive marine-shelf sequence.|1600-1200 Ma|Bangemall Group|Coodardoo, Ullawarra, Devil Creek, Kiangi Creek, Coobarra, Cheyne Springs, Top Camp, Irregully, Curran, Jillawarra, Tringadee Formations; Nanular, Gooragoora, Mount Augustus Sandstones; see Comments.|Unconformably overlies Gascoyne Complex. Is overlain conformably by Mucalana Subgroup. Is correlated with Scorpion Subgroup.||13-MAR-18
26264|Edmund Subgroup|50225|5|Briefly described|p387 Fig. 2|||Of Muhling and Brakel (1985). Formerly of the Bangemall Group - reassigned to the Dooley, Florry and Weegarinna Subgroups (Bangemall Group) - now superseded by Edmund Group.||||||07-FEB-11
26264|Edmund Subgroup|63869|6|Mentioned|p27|||Superseded name; raised to Group status following recognition of significant regional unconformity.||||||
26264|Edmund Subgroup|64772|6|Mentioned|p13|||Superseded by Edmund Group when Bangemall Basin stratigraphy was reviewed (Martin et al (1999).||||||07-FEB-11
79425|Edmund Subgroups|67201|6|Mentioned|p53 Fig.40|||Shown as Edmund Subgroups. Bangemall Basin.||||||
41228|Edmund group|50226|6|Mentioned|p427|||Informal - see Edmund Group.||||||
35378|Edna May orthogneiss|23200|6|Mentioned|p1016|||||||||
77174|Eel Creek Conglomerate|67827|6|Mentioned|p427 Fig.16|||See Eel Creek Formation (p427-428). ||||||
77174|Eel Creek Conglomerate|67829|6|Mentioned|p451.|||Northeast Pilbara.||||||
81332|Eelya Complex|70030|5|Briefly described|p190,192,205|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. Informal term used interchangeably with Eelya Suite in this study. See also Eelya Suite.||Unit of Annean Supersuite.||||
29432|Egna Sandstone|42933|5|Briefly described|Fig.94 p258|||Misspelling of Enga Sandstone.||||||
39270|Elang formation|24235|5|Briefly described|p298, p299|Jurassic|Jurassic|Informal name. Geological Province: Bonaparte Basin.||||||
24947|Elder Dolomite|30388|6|Mentioned|p11|||Refers Sofoulis(1962). Now Frank Scott Formation||||||
24947|Elder Dolomite|30390|6|Mentioned|p78|||Informal name previously applied to Frank Scott Formation||||||
32023|Elder Mountain Sandstone|43870|14|Not recorded|p100,299,322||Middle Cambrian|Palaeomagnetic readings. Age: 570-525 Ma. 16S 126E.||||||15-AUG-06
36942|Elders Subgroup|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|Of Goose Hole Group. Ord Basin.||||||
83644|Elephant Rocks dyke|73480|5|Briefly described|p217-218|Early Cretaceous|Early Cretaceous|Northeast striking dyke. Youngest concordant zircon grain dated is ca 940 Ma, also yielded discordant U/Pb ages of ca 250 Ma. Suggested to be associated with the Early Cretaceous Greater Kerguelen large igneous province.|ca 940 Ma U-Pb zircon maximum age, (<ca 250 Ma?)||||Unmetamorphosed dyke.|
38555|Eleven Mile Well Complex|24395|6|Mentioned|p201|||||||||
24264|Eley Adamellite|37633|4|Described|Table 41|||See also p27.||||||21-AUG-07
24264|Eley Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2.||||||07-NOV-08
24264|Eley Adamellite|39697|3|Fully described|p34|||||||||
24264|Eley Adamellite|44150|5|Briefly described|p143 Tb.2-21, p148 Fig.2-136|||Post-tectonic granitoid.||Shaw Granitoid Complex||Sharp contact with Cooglegong Adamellite.|Porphyritic biotite monzogranite, foliated.|
24264|Eley Adamellite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Superseded by Eley Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
68144|Elgee Formation|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
68144|Elgee Formation|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1704 +7/-14 Ma.|||||
68144|Elgee Formation|69003|6|Mentioned|p48 Fig.57|||Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.||||||
33009|Elgee Shale|44363|14|Not recorded|p.12|||Now named Elgee Siltstone in Kimberley Group.||||||
23576|Eliasson Formation|42615|3|Fully described|p33|Oxfordian|Oxfordian|Reserved.||||||27-NOV-09
78800|Eliot Range Formation|64104|5|Briefly described|p63 Fig.1, p76 fig 10, p77|Cryogenian|Tonian|See also reference to the currently formal name, Eliot Range Dolomite (p69). Formerly Bungle Bungle Dolomite.|c.1000-725 Ma.|Unit in Ruby Plains Group.||Is disconformably overlain by Duerdin Group.||
82821|Elisa Formation|72094|5|Briefly described|p12 Fig 9|Mesoproterozoic|Mesoproterozoic|Geological province: Bentley Basin inferred. [probable misspelling of Eliza Formation]||Of [Mount] Palgrave Group.|||Rhyolite|
69686|Elizabeth Hill Suite|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: 3093-3068Ma.  Geological Province: Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
68082|Ellendale lamproites|24568|5|Briefly described|p173|Miocene|Miocene|Informal name.  Youngest diamonds in Australia.  Age: ca. 20Ma.||||||06-APR-05
79738|Elm Sandstone|70934|5|Briefly described|unpaginated|Oxfordian|Oxfordian|Swan Graben, Vulcan Sub-basin. Slope-fan unit. Occurs as separate to partially-separate fault blocks in the Vesta oil and gas field, Swan Graben. Intersected by wells Vesta-1 and Vesta-2. Prospective reservoir target.||Lower Vulcan Formation||||24-JAN-17
32596|Elsie Creek granite|45923|14|Not recorded|p.46|||||||||
31394|Emanuel Shale|43581|6|Mentioned|p39|||||||||
31394|Emanuel Shale|63110|6|Mentioned|p1138|||Impermeable shale unit.||||||11-JUN-08
24951|Emanuel formation|35119|6|Mentioned|p467|||||||||
24951|Emanuel formation|41215|6|Mentioned|p265|||||||||
24951|Emanuel formation|43876|14|Not recorded|p553||Arenigian|||||||
40533|Emerald Mine Complex|24531|6|Mentioned|p41|||||||||
40533|Emerald Mine Complex|61252|6|Mentioned|p65|||May not be intended as a formal name? Highly deformed rocks.||||||
74680|Emerald Mine greenstone complex|64405|6|Mentioned|p17|||Informal name for a greenstone belt which apparently contains no Strelley Pool Formation, as do many of the other greenstone belts in the East Pilbara Terrane - 11 out of 20 have identified Strelley Pool Formation within them.||||||07-FEB-11
69673|Emiriau Sandstone|61155|5|Briefly described|p16|||May be misspelt - place name is Emeriau in W.A.  Age is pre-Cainozoic. Geological Province: Dampier Peninsula.||||||
38791|Empress Shale|23926|5|Briefly described|p9|Archean|Archean|Of Woolyeenyer Formation.  Geological Province: Yilgarn Craton.||||||07-NOV-08
32583|Empress Slate Member|45543|6|Mentioned|p.101-106|||Table 2.||||||
80095|Emu Pool Suite|70826|6|Mentioned|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Intrusion accompanied deposition of the Kelly Group.||||||12-MAY-20
69687|Emu Supersuite|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|Exposed only in the East Pilbara Granite-Greenstone Terrane. Age: 3.32-3.29Ga.  Geological Province: eastern Pilbara Craton. See also p54-55 Fig. 3.||||||07-NOV-08
42340|Enachedong Dolomite|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Misspelt. Of the Manganese Group (Bangemall Supergroup).||||||
42340|Enachedong Dolomite|66107|5|Briefly described|p4 Fig.1|Mesoproterozoic|Mesoproterozoic|||Of the Manganese Group||Overlies Stag Arrow Formation. Is overlain by Jigalong Formation.||
42340|Enachedong Dolomite|71042|4|Described|p66 fig 2|Mesoproterozoic|Mesoproterozoic|[Misspelling of Enacheddong]. See correct spelling p67.||Manganese Group||||28-MAY-19
32756|Enokurra Grit|45015|6|Mentioned|p30|||May be extension of Tumblagooda Sandstone. Geological Province: Irwin Basin.||||||31-MAY-06
42154|Enterprise dolerite|50551|5|Briefly described|p1094 Fig.5, p1097||Archean|Informal name. Intrudes Cashmans Sedimentary Horizon. In Eastern Goldfields Province.||||||07-NOV-08
42154|Enterprise dolerite|71166|6|Mentioned|p9 fig 3.4a, p19, p33|||Hosts mineralisation estimated at 1 Moz Au (Reserves, indicated and inferred).||||||
83934|Erawandoo Hill conglomerate|70316|6|Mentioned|p116, 118-120, 122, 125-127|||Jack Hills area. Contains Hadean-Eoarchean zircons aged 4.38-3.05 Ga. Also presented as Erawandoo Hill pebble conglomerate.|3.0-2.65 Ga.||||Upper greenschist facies pebble metaconglomerate.|
74600|Erayinia Granite Complex|60555|5|Briefly described|p9, p12, p14|Archean|Archean|Consists of quartz monzonite bodies. Age: c. 2660Ma and 2645+/-12Ma (Cassidy and Champion, 2002), ages from three granitic bodies form the complex.||||||07-NOV-08
74600|Erayinia Granite Complex|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean|Superseded by Erayinia Granitic Suite?|||||Syenogranite, quartz syenite, syenite, quartz monzonite.|05-AUG-15
75274|Erayinia Granitic Suite|65264|5|Briefly described|p25, p48 Appdx. 1|Archean|Archean|Ranges in composition from monzogranite to quartz syenite and syenite, typically with hornblende or clinopyroxene, and locally with abundant mafic xenoliths; massive to moderately foliated; strong shearing in mafic enclaves.||||||07-FEB-11
75274|Erayinia Granitic Suite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||Includes 3 unnamed subunits.||Syenite to monzogranite; hornblende or clinopyroxene bearing; massive to moderately foliated; strong shearing in mafic enclaves; quartz monzonite; commonly porphyritic.|05-AUG-15
75274|Erayinia Granitic Suite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Syenite to monzogranite; hornblende or clinopyroxene bearing; massive to moderately foliated; strong shearing in mafic enclaves. Quartz monzonite, locally porphyritic.|
75274|Erayinia Granitic Suite|70802|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Syenite to monzogranite; hornblende or clinopyroxene bearing; massive to moderately foliated; strong shearing in mafic enclaves, porphyritic quartz monzonite|
75274|Erayinia Granitic Suite|71168|5|Briefly described|p36||||||||Quartz monzonite; commonly porphyritic, schist, foliated granitic and subordinate foliated mafic rocks; quartz-rich monzogranite.|
75274|Erayinia Granitic Suite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Syenite to monzogranite; hornblende or clinopyroxene bearing; massive to moderately foliated; strong shearing in mafic enclaves; quartz monzonite; commonly porphyritic.|
24957|Erayinia Granitoid Complex|41771|4|Described|p30|||||||||
24957|Erayinia Granitoid Complex|42724|5|Briefly described|map legend|Archean||||||||07-NOV-08
24957|Erayinia Granitoid Complex|42817|5|Briefly described|p17|||||||||
24957|Erayinia Granitoid Complex|43222|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24957|Erayinia Granitoid Complex|43294|4|Described|p8||Archean|||||||07-NOV-08
24957|Erayinia Granitoid Complex|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
24957|Erayinia Granitoid Complex|60076|5|Briefly described|p46 App. 1|||[AgE]   Syenite to monzogranite; hornblende to clinopyroxene bearing; variable foliation.||||||
24957|Erayinia Granitoid Complex|64775|6|Mentioned|p6-1|Neoarchean|Neoarchean|Age from conventional U-Pb zircon method (not SHRIMP).| ~2636 Ma.|||||30-MAR-12
83180|Erayinia dykes|70017|5|Briefly described|p222-224, 226-228, 230|Paleoproterozoic|Paleoproterozoic|Kurnalpi Terrane, Eastern Goldfields Superterrane, SE Yilgarn Craton. E-NE trending dykes. All less than 4m thick. Paleomagnetic directions and poles tabulated. Siderian age. Too old to be part of the Marnda Moorn magmatic event, and ~10 m.y. younger than Widgiemooltha dyke swarm. ~11 degrees angular distance between the latter and Eraynia poles reflects ongoing plate tectonics between 2.45 and 2.2 Ga. Supercraton reconstructions discussed in detail.|2401 +/- 1 Ma (U-Pb TIMS baddeleyite).||||Mafic dykes, including very fine- to medium-grained dolerite.|
83180|Erayinia dykes|73057|6|Mentioned|p9|||Yilgarn Craton. E- to ENE-trending dykes. See also Eraynia dykes, Erayinia dyke swarm.||||||
83181|Eraynia dykes|73057|6|Mentioned|p4, p8 Fig.7|Siderian|Siderian|Yilgarn Craton, eastern. See also Erayinia dykes and Erayinia dyke swarm.|2401+/-1 Ma|Widgiemooltha Supersuite||||
31762|Errabiddy Formation|23569|4|Described|p4 Tb. 1|Proterozoic|Proterozoic|Formerly Errabiddy Sandstone.   Parent: Badgeradda Group.   Feldspathic sandstone; minor pebble-conglomerate lenses||||||
31762|Errabiddy Formation|24114|5|Briefly described|p8|Neoproterozoic|Mesoproterozoic|Of Badgeradda Group. Geological Province: Yilgarn Craton.||||||
31762|Errabiddy Formation|43835|5|Briefly described|Map Legend||Proterozoic|of Badgeradda Group.||||||
31762|Errabiddy Formation|69583|5|Briefly described|p130, Plate 3|Proterozoic|Proterozoic|Badgeradda Basin.||Badgeradda Group.|||Feldspathic sandstone; minor pebble conglomerate lenses.|
31762|Errabiddy Formation|70795|4|Described|500k_interpgeop14_lut.csv|Neoproterozoic|Mesoproterozoic||1091-541 Ma inferred.|Badgeradda Group|||Feldspathic sandstone; minor pebble conglomerate lenses.|25-SEP-17
31762|Errabiddy Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
31762|Errabiddy Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Badgeradda Basin.||Badgeradda Group|||Feldspathic sandstone; minor pebble conglomerate lenses.|
80351|Erramurra Monzogranite|70775|5|Briefly described|p15, p53|Mesoarchean|Mesoarchean|Together with the Miaree Granite and the Hearson Cove Monzogranite forms the Dampier Granitic Complex. This unit is poorly exposed over an area of 10km^2. |2982 +/- 5 Ma (Nelson, 1999i)|Maitland River Supersuite|||Seriate biotite monzogranite, containing mafic schlieren and veins of pegmatite.|
33037|Erskine Formation|24062|5|Briefly described|p186 Table 1|Triassic|Triassic|Geological Province: Canning Basin.||||||
33037|Erskine Formation|44006|14|Not recorded|p65|||Part of Derby Group.||||||
75590|Eskdale Member|61555|6|Mentioned|Fig. 5 p239|||?of Barrow Group.||||||
75590|Eskdale Member|70066|5|Briefly described|Regional: Fig.6|Tithonian|Kimmeridgian|Exmouth Sub-basin, Northern Carnarvon Basin.||Dupuy Formation.||||
30533|Esperance Granite|22448|6|Mentioned|p876|||||||||
30533|Esperance Granite|24165|5|Briefly described|Plate 1|Mesoproterozoic|Mesoproterozoic|||Nornalup Complex.|||Weakly to moderately deformed and recrystallised granite; even-grained or porphyritic.|
30533|Esperance Granite|24526|5|Briefly described|p105 Fig. 6, p108|Mesoproterozoic|Mesoproterozoic|Of the Nornalup Complex. Porphyritic granite.  Age: >1100Ma.||||||
30533|Esperance Granite|43203|5|Briefly described|Map Legend||Proterozoic|Of Nornalup Complex||||||
30533|Esperance Granite|43498|4|Described|5,7|||aged: 1100- 1200Ma||||||
30533|Esperance Granite|62381|5|Briefly described|p3 Fig.3, p7.|||Late-tectonic; porphyritic.|c.1140 Ma.|Unit in Nornalup Complex.||||03-JUL-14
30533|Esperance Granite|63866|5|Briefly described|p190, p192|||Nornalup Complex. Metamorphic ages include 1138 +/- 38 Ma and 1135 +/- 56 Ma (U-Pb zircon, Nelson, 1996).|c. 1140 Ma|||||
30533|Esperance Granite|64580|4|Described|map legend||Mesoproterozoic|Weakly to moderately deformed and recrystallized granite; even grained or porphyritic.||||||15-DEC-08
30533|Esperance Granite|65487|6|Mentioned|p1, p9, 41|||Myers (1995), Nelson et al. (1995). Relatively undeformed, low metamorphic grade granitic rocks intruding Recherche Supersuite. Renamed as the Esperance Supersuite.||||||
30533|Esperance Granite|67581|6|Mentioned|p44 Fig.8|||||||||
30533|Esperance Granite|68186|5|Briefly described|p4, p27-28|||Myers (1995). Subsequently renamed the Esperance Supersuite.|||||Defined as comprising relatively undeformed, low metamorphic grade granitic rocks that intruded the Recherche Granite.|
30533|Esperance Granite|69152|5|Briefly described|500k_geologyp08_lut||Mesoproterozoic||||||Weakly to moderately deformed and recrystallized granite; even grained or porphyritic.|05-AUG-15
30533|Esperance Granite|69252|6|Mentioned|p4 Fig.1, p20|||Myers (1995). Subsequently the Esperance Supersuite.||||||
30533|Esperance Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
35827|Esperance-Biranup Complex|23320|6|Mentioned|p426 Fig.6|||Informal compound term.||||||07-FEB-07
24962|Eucla Limestone""|32552|6|Mentioned|p60|||See also P76, 87. Refers Maitland (1901) & Fairbridge (1953).||||||
24962|Eucla Limestone""|65942|6|Mentioned|p74|||||||||
70223|Eundyne Group|24410|5|Briefly described|p130 Fig. 75|Cenozoic|Cenozoic|Sandstone, siltstone, mudstone. ||||||19-NOV-08
80633|Eundynie Group""|71788|6|Mentioned|p97 |||Includes Norseman Lst, Cowan Dolomite and Princes Royal Spongolite. Introduction of new name. used without quotes elsewhere in article.||||||
42444|Eurada gneiss|60694|5|Briefly described|p253, p273|Archean|Archean|Informal name.  Age: 3490-3440Ma (zircon).   Geological Province: Narryer Terrane/Yilgarn Craton.||||||07-NOV-08
42444|Eurada gneiss|64771|5|Briefly described|p7|||||||Intrudes Meeberrie Gneiss and Manfred Complex.|Felsic magmatic intrusions.|
42444|Eurada gneiss|66583|5|Briefly described|p806|Paleoarchean|Paleoarchean|Geological province: Yilgarn Craton. Of the Narryer Gneiss Complex. Tonalitic to granitic magmas (protoliths) were emplaced at. 3.49-3.44 Ga. Contains 3.30-3.28 Ga zircons, interpreted to reflect metamorphism caused by granties emplacement.||||||
42444|Eurada gneiss|71802|6|Mentioned|p288||||3490-3440 Ma||||Granitic to tonalitic gneiss.|
82824|Eureka basalt|72095|6|Mentioned|p9, 10|||Eastern Goldfields, Yilgarn Craton. Probably volcanic equivalent of Eureka Dolerite? See discussion p21.||||||
38818|Eureka-Federal Dolerite|23928|5|Briefly described|p66|Archean|Archean|Max. thickness: 100m.  Geological Province: Yilgarn Craton.||||||07-NOV-08
73846|Euro Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group). Tholeiitic and komatiitic pillow basalt and chert. Max. thickness 9.4km.||||||07-FEB-11
73846|Euro Formation|60636|5|Briefly described|p44, p38 Fig. 3.3|Archean|Archean|Misspelt? See also Euro Basalt. Serpentised and carbonitised massive basalt. Overlies the Panorama Formation. Age: 3346Ma. See also p35-36 Fig. 3.2.||||||07-FEB-11
73846|Euro Formation|62427|5|Briefly described|p3 Fig.2, p5, p6 Fig.3|||Of Williams (1999). See Euro Basalt.||Of the Warrawoona Group|||Silicified basalt and minor intercalated thin-bedded chert.|
73846|Euro Formation|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
38663|Extension Tank monzogranite|23786|5|Briefly described|p56|||Informal name.  Geological Province: Yilgarn Craton.||||||
40186|F sand""|23520|6|Mentioned|p32|||Informal name for the intra-Cattamarra Coal Measures Sandstone.||||||
23586|Fair Adelaide Granite|22534|6|Mentioned|p12|||||||||
23586|Fair Adelaide Granite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
23586|Fair Adelaide Granite|42705|5|Briefly described|map legend|Archean||Variation on Fair Adelaide Syenogranite. Name now as originally reserved.||||||07-NOV-08
23586|Fair Adelaide Granite|42988|5|Briefly described|Map Legend|||||||||
23586|Fair Adelaide Granite|42989|6|Mentioned|p11|||||||||
23586|Fair Adelaide Granite|43101|5|Briefly described|p25|||||||||
23586|Fair Adelaide Granite|43102|5|Briefly described|Fig.4|||||||||
23586|Fair Adelaide Granite|43214|6|Mentioned|Map Legend||Archean|||||||07-NOV-08
26545|Fairfield Formation|22550|6|Mentioned|Fig 3|||||||||
26545|Fairfield Formation|22767|6|Mentioned|P20|||Probably equivalent to the Luluigai Formation, seperseded by the Fairfield Group||||||
26545|Fairfield Formation|24061|5|Briefly described|p180|||Geological Province:  Canning Basin.||||||
26545|Fairfield Formation|24062|5|Briefly described|p186 Table 1|Devonian|Devonian|Geological Province: Canning Basin.||||||
26545|Fairfield Formation|30110|6|Mentioned|p81|||Tournaisian age.||||||
26545|Fairfield Formation|30525|6|Mentioned|Map legend|Tournaisian|Famennian|Famennian to Tournaisian.||||||
26545|Fairfield Formation|30533|4|Described|p24|||On Table 6. Includes "Laurel Formation" & "Fairfield Beds"||||||
26545|Fairfield Formation|30682|6|Mentioned|p72|||||||||
26545|Fairfield Formation|30897|4|Described|p18|||||||||
26545|Fairfield Formation|30898|6|Mentioned|Map legend|Tournaisian|Famennian|Famennian - Tournaisian||||||
26545|Fairfield Formation|31150|6|Mentioned|p98|||Refers Balme & Hassell (1962)||||||
26545|Fairfield Formation|31152|6|Mentioned|Fig. 3|||||||||
26545|Fairfield Formation|31332|6|Mentioned|Fig. 3|||||||||
26545|Fairfield Formation|32594|6|Mentioned|p3|||||||||
26545|Fairfield Formation|32638|6|Mentioned|p22|||Trilete spores in wells.||||||
26545|Fairfield Formation|32640|6|Mentioned|p241|||||||||
26545|Fairfield Formation|32641|6|Mentioned|p10|||L.Carb.||||||
26545|Fairfield Formation|32647|6|Mentioned|p98|||||||||
26545|Fairfield Formation|32648|6|Mentioned|p32|||||||||
26545|Fairfield Formation|33042|6|Mentioned|Fig.2|||See also PP 725 & 738.||||||
26545|Fairfield Formation|33621|6|Mentioned|p183|||Famennian||||||
26545|Fairfield Formation|34085|6|Mentioned|Cor.chart|||Famennian||||||
26545|Fairfield Formation|34427|6|Mentioned|Fig.3|||||||||
26545|Fairfield Formation|35104|6|Mentioned|Fig.2|||||||||
26545|Fairfield Formation|35275|6|Mentioned|Fig.5.|||||||||
26545|Fairfield Formation|36890|3|Fully described|p335|||Formerly Fairfield Marl,Fairfield Beds. Includes Laurel Fm.||||||
26545|Fairfield Formation|40793|6|Mentioned|p167|||||||||
26545|Fairfield Formation|40837|6|Mentioned|Fig.14|||||||||
26545|Fairfield Formation|41215|6|Mentioned|p263|||||||||
26545|Fairfield Formation|41839|6|Mentioned|p21|||Superseded by Fairfield Group||||||
26545|Fairfield Formation|42111|5|Briefly described|p88|||See also Text fig.3||||||
26545|Fairfield Formation|43815|6|Mentioned|Table 1,p95-96|||||||||
26545|Fairfield Formation|44040|14|Not recorded|p43|||||||||
26545|Fairfield Formation|44397|14|Not recorded|p.12,20, Fig.2,3,Tb4||Famennian|See also p.13,18.||||||
26545|Fairfield Formation|44398|14|Not recorded|map legend||Famennian|||||||
26545|Fairfield Formation|44994|6|Mentioned|Fig.6|||Correlation. Famennian.||||||
26545|Fairfield Formation|44998|14|Not recorded|p.43|||||||||
26545|Fairfield Formation|45015|5|Briefly described|p59|Devonian|Devonian|Probably same age as Willaraddie Formation. Geological Province: Fitzroy Basin.||||||01-JUN-06
26545|Fairfield Formation|45039|6|Mentioned|p21|||Upper Devonian. See Fig.5.||||||
26545|Fairfield Formation|45041|6|Mentioned|Fig.45|||U.Dev. - L.Carb.||||||
26545|Fairfield Formation|45056|6|Mentioned|p58|||||||||
26545|Fairfield Formation|45063|6|Mentioned|p14|||See also P28 & Fig. 9. Devonian||||||
26545|Fairfield Formation|45101|6|Mentioned|p7|||Conodont content||||||
26545|Fairfield Formation|45133|6|Mentioned|Fig.8|||||||||
26545|Fairfield Formation|45143|4|Described|p4|||Discussion on origin of term.||||||
26545|Fairfield Formation|45153|6|Mentioned|App.3-57|||||||||
26545|Fairfield Formation|46849|6|Mentioned|p182|||See also Fig. 2||||||
26545|Fairfield Formation|46912|6|Mentioned|Table 1|||Analytical data of Canning Basin cores||||||
26545|Fairfield Formation|47050|6|Mentioned|p251|||||||||
26545|Fairfield Formation|65382|6|Mentioned|p717 App. 2|Tournasian|Tournasian|Canning Basin. 350 Ma.||||||
26545|Fairfield Formation|73117|6|Mentioned|p120|||[Superseded/variation of published name; see Fairfield Group].||||||
24972|Fairfield marl""|41215|6|Mentioned|p278|||||||||
69660|Fantome Formation""|61155|5|Briefly described|p15, p16||Late Oligocene|Max. thickness: 1500m in Sahul Platform region. Geological Province: Bonaparte Basin / Ashmore and Sahul Platforms, Vulcan and Petrel Sub-basins, and the Bonaparte-Money Shoal Basin - north. ||||||
28547|Fargo Tillite|36551|6|Mentioned|Table 12|||Misspelling of Fargoo?||||||
74156|Fargoo Formation|63762|5|Briefly described|p20|||Massive diamictite. See also Fargoo Tillite.||||||07-FEB-11
74156|Fargoo Formation|64104|4|Described|p61-80|Neoproterozoic|Neoproterozoic|The author proposes this name replace Fargoo Tillite "to distinguish stratigraphic terms from genetic interpretation". Records continental glaciation. Provenance discussed.||Duerdin Group||Overlies Skinner Sandstone. Is overlain conformably by Frank River Sandstone.|Diamictite: characteristic green matrix, boulders of granite and indurated sandstone, typically faceted, polished and striated; and conglomerate: abundant carbonate clasts in a calcareous/sand matrix.|
74156|Fargoo Formation|67484|6|Mentioned|p294|Cryogenian|Cryogenian|East Kimberley. ||||Shown as being overlain by Frank River Sandstone.||
74156|Fargoo Formation|67620|5|Briefly described|p5|Cryogenian|Cryogenian|East Kimberley region.||Duerdin Group.||Is overlain by Frank River Sandstone.||
74156|Fargoo Formation|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region. Considered as equivalent of the Elatina glaciation.||Duerdin Group.||||
74156|Fargoo Formation|68244|4|Described|p659-660,666-671|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Glaciogenic unit deposited during of Landrigan Glaciation.  High carbonate content likely due to erosion and remobilisation through glacial avtivity from underlying Bungle Bungle Dolomite, Eliot Range Doloite and Olympio Formation. Shown as Fargoo Tillite on p667.||Unit of Duerdin Group.||Lowermost unit of Duerdin Group. Overlain by Frank River Sandstone.   Correlative to Walsh Fm (Mount House Gp), and Landrigan Fm (Kuniandi Group).|Rounded and weathered ridges of mostly massive diamictite with a characteristic green matrix; conglomerate and sandstone interbedded with stratified and massive diamictite, massive clast-rich and gradeddiamictite facies.|
74156|Fargoo Formation|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
38973|Fargoo-Moonlight Valley tillite|23806|6|Mentioned|p1121|Neoproterozoic|Neoproterozoic|Informal compound name  - see also Fargoo Tillite and Moonlight Valley Tillite.||||||18-SEP-06
82277|Faure Sandstone Member""|69558|6|Mentioned|p106|Pleistocene|Pleistocene|Of Playford and Berry (2002). Replaced by Hoult Sandstone Member.||Peron Sandstone||||
39887|Federal granodiorites|24596|6|Mentioned|p561|Archean|Archean|Informal name for granites of the Federal open pit deposit.  Geological Province: Yilgarn Craton.||||||07-NOV-08
78862|Fiddlers Lake Granite|66129|6|Mentioned|p216 Fig.3|Statherian|Statherian|~1730-1735 Ma.||||||15-MAY-14
78862|Fiddlers Lake Granite|70291|4|Described|p180|Statherian|Statherian|Geological province: Arunta region. Coeval with (or intrudes?) Pargee Sandstone deposition.|~1730 Ma||||S-type granites and migmatites.|
78862|Fiddlers Lake Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1740+/-5 Ma (metamorphism: U-Pb zircon SHRIMP)||||Granite.|
23590|Fields Find Group|41066|6|Mentioned|1 of 2 K05|||||||||
75936|Finke beds|64625|6|Mentioned|p254|||Name replaced by Johnnys Creek beds.||||||
75936|Finke beds|64797|6|Mentioned|p154 Fig.5|||||||Overlies Bitter Springs Formation.||
75936|Finke beds|65365|5|Briefly described|p9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Amadeus Basin. Overlies Loves Creek Member of the Bitter Springs Formation. Unconformably overlain by Areyonga Formation.||||||
75936|Finke beds|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Amadeus Basin. Overlies Loves Creek Member of the Bitter Springs Formation.  Unconformably overlain by Areyonga Formation.||||||
75936|Finke beds|69438|5|Briefly described|p23:2-3, 14-15, 18, 59-60|Cryogenian|Cryogenian|Amadeus Basin. Has been used interchangeably with Johnnys Creek beds, or has been considered replaced by that name. Recent work indicates that it has a distinct and significant biostratigraphic succession and warrants formalisation as a separate unit. Has promising Neoproterozoic hydrocarbon reservoirs.||||Unconformably overlies Bitter Springs Formation. Is overlain unconformably by Inindia beds or Areyonga Formation.|Various shades of grey and pale pink, white and pink-grey dolostone, micritic to finely sucrosic in grain size, with minor pyrite and anhydrite; also contains minor to abundant chert and is often silty, becoming dolomitic siltstone in part.|12-JUL-16
75936|Finke beds|69606|5|Briefly described|p1, p8, p10, p19|||Informal unit, considered inappropriate becaues the Finke Group is already an established stratigraphic unit in the Amadeus Basin. Correlates with an unnamed unit beneath the Areyonga Formation. Distinctive acritarch fossils of Cerebrosphaera Buickii and stromatolite Bacalia burra. ||||Correlates with the Burra Group and the upper Buldya Group. Locally overlies the Loves Creek Member.|Interbedded sandstone, ooid and stromatolitic carbonate (mainly dolostone) and red, green and black siltstone, and shale.|
75936|Finke beds|69673|5|Briefly described|p64 fig 53, p84, p85, p90, p91|||At times used interchangeably with Johnnys Creek beds.||||Unconformably overlies Johnnys Creek beds, unconformably overlain by Inindia beds, Areyonga Formation|Micritic to sucrosic dolostone with minor to abundant chert and dolomitic siltstone.|
75936|Finke beds|70416|6|Mentioned|p64, p65 Fig.2|Cryogenian|Cryogenian|Informal; name replaced by Wallara Formation.||||||
75936|Finke beds|72375|6|Mentioned|p15|||Of Amadeus Basin. Superseded, see Wallara Formation.||||||
75936|Finke beds|72601|6|Mentioned|p7|||Formalized as Wallara Formation.||||||
75936|Finke beds|73085|6|Mentioned|p1, p27|||Superseded by Wallara Formation. [Written as 'Finke beds'].||||||
75936|Finke beds|73086|6|Mentioned|piii, p5, p39, p56-57, p156|||Superseded [see Wallara Formation]. [Also written as 'Finke beds'].||||||
75936|Finke beds|73088|6|Mentioned|p1|||Superseded; see Wallara Formation.||||||
78329|Finlay intrusion|65135|5|Briefly described|p14|||Informal name. Broadly troctolitic. Of the Giles intrusions. Probably part of a larger single intrusion including the Blackstone, Jameson and Bell Rock intrusions.||||||
26553|Finlayson Formation|22493|6|Mentioned|p100|||||||||
26553|Finlayson Formation|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26553|Finlayson Formation|40989|6|Mentioned|p13|||||||||
26553|Finlayson Formation|43238|5|Briefly described|p6|||||||||
26553|Finlayson Formation|49896|5|Briefly described|p6|||Comprises the former Finlayson Formation, Doolgunna, Thaduna and Maraloou Formations as well as the newly defined Killara Formation. See also Finlayson Sandstone - names used interchangeably in this study.||||||23-APR-09
29995|Finlayson Sandstone Member|12099|6|Mentioned|p678 Fig.4|||Obsolete name. Equivalent to Finlayson Sandstone of Gee (1987), and Finlayson Member of Occhipinti et al. (1997), Pirajno et al. (1998) and this paper?  Placed in Glengarry Group by Gee and Grey (1993)||Unit in Juderina Formation.||||04-MAR-13
29995|Finlayson Sandstone Member|23744|6|Mentioned|p10|||Replaced by Finlayson Member.||||||
29995|Finlayson Sandstone Member|23749|6|Mentioned|p6|||Superseded by Finlayson Member||||||
29995|Finlayson Sandstone Member|43069|1|Redefined|p30|Mesoproterozoic|Paleoproterozoic|of Juderina Formation. Supersedes Finlayson Sandstone||||||07-NOV-08
29995|Finlayson Sandstone Member|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Gee and Grey (1993); Of Juderina Formation. See also Finlayson Sandstone and current Finlayson Member.||||||
29995|Finlayson Sandstone Member|65419|5|Briefly described|p8, p14.|Paleoproterozoic|Paleoproterozoic|Gee and Grey (1993) incorporated the quartz arenite at the southern end of the Glengarry Basin as the Finlayson Sandstone Member of the Juderina Formation. Renamed the Finlayson Member (Occhipinti et al. 1997) because of its heterolithic nature.||Unit in Juderina Formation.||||
36891|Finlayson Sandstone""|23586|6|Mentioned|p15|||Now known as Juderina Formation.||||||
36891|Finlayson Sandstone""|23759|5|Briefly described|p15|||Replaced by Juderina Formation.||||||
76070|Finlayson member|65408|5|Briefly described|pp82-83.|Paleoproterozoic|Paleoproterozoic|Typo for Member.||Unit in Juderina Formation.|||Shallow-water arenite.|20-SEP-11
38810|Fisher basalt|23931|6|Mentioned|p201 Table 1|||Informal name - see Fisher Basalt. Geological Province: Yilgarn Craton.||||||
38810|Fisher basalt|60979|5|Briefly described|p86 Fig.2, p90, p92|||Informal name. Part of the Jundee sequence in the Jundee goldfield area. Overlies the Plover Bore komatiite. Geological Province: Yilgarn Craton. Massive and pillowed tholeiitic basalt.||||||27-JUN-05
81148|Fitzgerald Brown Coal Series""|71789|6|Mentioned|p99|||Of Blatchford (1930) for lignite in Fitzgerald River area. Now included in Werillup Formation.||||||
80206|Fitzroy Mylonite|70482|6|Mentioned|p323-324, 326-327|Archean|Archean|Fitzroy Structural Zone, associated with the Scotia-Kanowna Dome, Eastern Yilgarn Craton.|||||High-strain pods or lozenges preserved in later lower strain thrust fabrics.|
80206|Fitzroy Mylonite|71166|6|Mentioned|p122|||||||Intruded by the Kanowna Belle porphyry.||
80206|Fitzroy Mylonite|73238|5|Briefly described|p18, 20-21|||Associated with the Fitzroy Fault, Kalgoorlie district. Eastern Goldfields Terrane. Deformation structures described.||||||10-JAN-23
69129|Fitzroy mylonite|60514|6|Mentioned|p49|||Informal name.||||||07-FEB-11
69129|Fitzroy mylonite|60625|6|Mentioned|p47|||Informal. Geological Province: Eastern Goldfields.||||||
38169|Fitzroy volcanics|23766|5|Briefly described|p13 Tb. 2|Tertiary|Tertiary|Informal - see Fitzroy Volcanics||||||
76855|Flacourt Sands|12466|6|Mentioned|p179.|Early Cretaceous|Early Cretaceous|[Formal name is Flacourt Formation]. Reservoir for paraffinic, medium gravity oils at the edge of the Barrow Sub-basin.||||||08-MAY-12
79823|Flames Porphyry|67198|6|Mentioned|p119 Fig.53|||Victory-Defiance area, St Ives goldfield.||||||
79823|Flames Porphyry|68289|6|Mentioned|p29-p31||||c. 2658 +/- 4 Ma (Nguyen, 1997)|||||
79823|Flames Porphyry|69631|5|Briefly described|p25, p27-28|Neoarchean|Neoarchean|Part of the greenstone succession at the Leviathan (Victory-Defiance) gold deposit. Mentioned as constituting an informal suite, forming a series of NW-trending, subvertical to steeply dipping sheets. Is boudinaged by the Repulse Fault. Gold mineralisation occurs at the intersection of this unit with the Repulse Fault. Appears as Flames Porphyry suite on p25 and Flame Porphyry on p28.|2658 +/- 4 Ma (Nguyen, 1997).|||||19-JUN-17
69184|Flames porphyry|60514|6|Mentioned|p36|||Informal name.||||||07-FEB-11
69184|Flames porphyry|60623|6|Mentioned|p36|||||||||
77108|Flamingo Sandstone|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Late Jurassic|Northern Bonaparte Basin.||||||
77108|Flamingo Sandstone|68223|6|Mentioned|p178 Fig.3|Berriasian|Tithonian|||||||
32676|Flapper Hill Sandstone|44965|14|Not recorded|Not recorded|||||||||
32676|Flapper Hill Sandstone|45038|14|Not recorded|Not recorded|||||||||
82945|Flat Rock Sandstone|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||Albert Edward Group||Overlies the Nyuless Sandstone, disconformably underlies the Kinevans Sandstone.||
69688|Flat Rocks Suite|61253|6|Mentioned|p51|||Same as Flat Rocks Supersuite, or part of it? Granitoid rocks.||||||31-AUG-05
69689|Flat Rocks Supersuite|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|See also Flat Rocks Suite.  Age: 3170-3160Ma.  Geological Province: Pilbara Craton.  See also p54-55 Fig. 3.||||||07-NOV-08
81302|Fleece Pool gabbro|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Yalgowra Suite.||||
81302|Fleece Pool gabbro|73596|6|Mentioned|p1160|Neoarchean|Neoarchean|Kalgoorlie Terrane. Presented as Fleece Pool layered gabbro.|2735 +/- 5 Ma.|||||
31886|Fletcher Creek Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1865Ma.||||||07-NOV-08
31886|Fletcher Creek Monzogranite|23751|5|Briefly described|p14|||||||||
31886|Fletcher Creek Monzogranite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tickalara Metamorphics (Lamboo Complex).  Age: 1865-1850Ma.||||||07-NOV-08
31886|Fletcher Creek Monzogranite|43854|5|Briefly described|Map Legend||Proterozoic|of Tickalara Metamorphics.||||||
31886|Fletcher Creek Monzogranite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31886|Fletcher Creek Monzogranite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31886|Fletcher Creek Monzogranite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Tickalara Metamorphics. Age: c. 1850Ma. Foliated and metamorphosed, leucocratic, biotite-muscovite (-garnet-magnetite) monzogranite; contains rounded to angular inclusions of amphibolite and country rock.||||||
31886|Fletcher Creek Monzogranite|63866|5|Briefly described|p131|||Central Zone, Halls Creek Orogen.||||Intrudes the Tickalara Metamorphics.||
31886|Fletcher Creek Monzogranite|66845|4|Described|p538, p539 Tb.1, p540, p541 Fig.7|||Protoliths of Tickalara Metamorphics were intruded by leucogranite sheets, named Rose Bore Granite and Fletcher Creek Monzogranite ("Eastern Leucocratic Granitoid" of Ogasawara, 1988). This unit truncates S1 layering and intruded before or during high-grade regional metamorphism and deformation (D2) at 1850-1845 Ma. The Dougalls Tonalite and Fletcher Creek Monzogranite have the same crystallisation age, and are part of a widespread magmatic event in the Central zone of the Lamboo Complex at c. 1850 Ma.|interp. igneous cryst'n age 1850+/-2Ma SHRIMP U-Pb||||quartz, oligoclase, and microcline, minor garnet, biotite, muscovite and iron-oxides (Ogasawara 1988); garnet-biotite syenogranite; leucogranite|
31886|Fletcher Creek Monzogranite|72437|6|Mentioned|p6|Palaeoproterozoic|Palaeoproterozoic|Said to be the Eastern Leucocratic Granitoid of Ogasawara (1988). Sheppard et al (1995) included it within the Dougalls suite; however the present authors have excluded it due to differing chemistry.||||||
31901|Foal Creek Intrusion|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
31901|Foal Creek Intrusion|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31901|Foal Creek Intrusion|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.||||||15-DEC-08
37835|Fohn lamproites|24218|4|Described|p855|||Informal name.   Geological Province: Bonaparte Basin.||||||
32744|Fontainebleau siltstone|44998|14|Not recorded|p266|||? Permian||||||
24986|Footwall Sandstone|41892|6|Mentioned|Fig.3|||||||||
24986|Footwall Sandstone|42730|6|Mentioned|Fig 13, P17|||||||||
24986|Footwall Sandstone|43278|5|Briefly described|p344,Fig.3.|Neoproterozoic|Neoproterozoic|Telfer mine sequence.||||||
24986|Footwall Sandstone|43867|5|Briefly described|Fig.3 p201|||Informal unit of the Telfer mine sequence.||||||
24986|Footwall Sandstone|43868|5|Briefly described|Fig.2 p153|||||||||
24986|Footwall Sandstone|44139|6|Mentioned|p281 Table 3-15|||Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation and later in Malu Formation..| | ||||10-SEP-12
77182|Footwall Sandstone Member|44139|6|Mentioned|p281 Table 3-15|||Of Upper Malu Formation (1983). Informal name (of Turner 1983 PhD thesis). Included in Telfer Formation in 1982.| | ||||10-SEP-12
40063|Forestier Bay Tonalite|23936|5|Briefly described|Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 3015 Ma.||||||07-NOV-08
40063|Forestier Bay Tonalite|61267|5|Briefly described|p71, p73 Tb.1|Archean|Archean|Age: c. 3015 Ma. Biotite-hornblende trondhjemite. Geological Province: Pilbara Craton.||||||07-NOV-08
33913|Forestier Bay gneiss|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3014 Ma||||||07-NOV-08
40087|Forestier Claystone Formation|24208|5|Briefly described|p174|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin.||||||
77457|Forestier Formation|67369|6|Mentioned|p247.|Cretaceous|Cretaceous|Elsewhere in this article the formal name, Forestier Claystone, is used. Forms a seal over the Pluto Gas Field.|||||Shales.|
81857|Forrest Sandstone|70772|6|Mentioned|p33 Table 2|||See also p37, which shows that the samples from Well FOR010 labelled Forrest Sst in Table 2 are part of the Decoration Sandstone.||||||06-MAY-20
34537|Forrestania Greenstone Belt|22775|3|Fully described|7|||||||||
73577|Forrestier Bay Granodiorite|63441|5|Briefly described|p10 Tb. 2, p36|Archean|Archean|Probably misspelt - W.A. spelling for this bay is Forestier Bay. Of the Orpheus Supersuite - within the structure of Harding Granitic Complex. Age: 3014+/-3Ma. Geological province: Pilbara Craton. See also p37.||||||07-FEB-11
73577|Forrestier Bay Granodiorite|64580|4|Described|map legend||Mesoarchean|Of Orpheus Supersuite. Biotite granodiorite and monzogranite; sparsely porphyritic; metamorphosed.||||||15-DEC-08
73577|Forrestier Bay Granodiorite|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Orpheus Supersuite.|||Biotite granodiorite and monzogranite; sparsely porphyritic; metamorphosed|
34485|Forsyth's Conglomerate|22769|5|Briefly described|Table1p759||Middle Eocene|See also Forsyths Conglomerate mentioned as a 'basal conglomerate' - a member perhaps?  This version of the name is probably a misspelling.||||||17-JAN-06
40073|Fortescue Group, lower|24541|6|Mentioned|p2|||Not intended as a formal name.||||||
40073|Fortescue Group, lower|61259|6|Mentioned|p403, p408|Archean|Archean|Informal - see Fortescue group.||||||07-NOV-08
76835|Fortescue Volcanics|67027|6|Mentioned|p350.|||Includes the older termed Nullagine Volcanics.||||||
24988|Fortescue metabasalt|39644|6|Mentioned|p1|||||||||
34985|Fortescue volcanics|23033|5|Briefly described|157|||||||||
39757|Fortesque Formation|24194|6|Mentioned|p906 Fig.6|||Misspelt - see Fortescue Group. Geological Province: Pilbara Craton||||||
42353|Fortesque Group|60539|5|Briefly described|p498 Fig.1|Paleoproterozoic|Archean|Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton. Misspelt, see Fortescue Group.||||||07-NOV-08
42353|Fortesque Group|62986|5|Briefly described|p18|Mesoarchean|Mesoarchean|Probably misspelt? (should be Fortescue?). Includes the Hardy Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
79792|Forty-four Hill Member|68574|6|Mentioned|p3|||||Lizard Hills Formation.||||
26559|Fossil Cliff Formation|15881|5|Briefly described|p62|Early Permian|Early Permian|Conformabe on/interfingers with Holmwood Shale; overlain by High Cliff Sandstone; however, subsequent interpretation placed it within Holmwood Shale as Fossil Cliiff Member. Fossiliferous limestones, dark siltstone, sandy siltstone + shale. Perth Basin.||||||
26559|Fossil Cliff Formation|23815|6|Mentioned|p281|Sakmarian|Sakmarian|Geological Province: Perth Basin.||||||
26559|Fossil Cliff Formation|23816|4|Described|p232|Sakmarian|Sakmarian|Formerly known as the Fossil Cliff Beds"". Geological Province: Perth Basin. Underlying unit: Holmwood Shale (conformable). Overlying unit: High Cliff Sandstone (conformable). Max. thickness: 45 m. Richly fossiliferous.||||||
26559|Fossil Cliff Formation|29548|6|Mentioned|p230|||||||||
26559|Fossil Cliff Formation|30545|6|Mentioned|Fig.2|||Sakmarian age. See also P22||||||
26559|Fossil Cliff Formation|30973|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
26559|Fossil Cliff Formation|31037|6|Mentioned|p1031|||Sakmarian Metalegocem's Kayi n. sp.||||||
26559|Fossil Cliff Formation|31561|6|Mentioned|p5|||See also P18. Stratigraphic column||||||
26559|Fossil Cliff Formation|32337|4|Described|p24|||||||||
26559|Fossil Cliff Formation|32648|6|Mentioned|p32|||L. Perm||||||
26559|Fossil Cliff Formation|32945|6|Mentioned|p73|||See also P88. Sakmarian||||||
26559|Fossil Cliff Formation|33052|6|Mentioned|Fig.1|||Sakmarian||||||
26559|Fossil Cliff Formation|33627|6|Mentioned|p582|||||||||
26559|Fossil Cliff Formation|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
26559|Fossil Cliff Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
26559|Fossil Cliff Formation|34287|6|Mentioned|p123|||||||||
26559|Fossil Cliff Formation|34532|6|Mentioned|Fig.2|||||||||
26559|Fossil Cliff Formation|34570|6|Mentioned|p115|||||||||
26559|Fossil Cliff Formation|35268|6|Mentioned|p22|||||||||
26559|Fossil Cliff Formation|35492|6|Mentioned|p145|||||||||
26559|Fossil Cliff Formation|35873|6|Mentioned|p82|||||||||
26559|Fossil Cliff Formation|36020|6|Mentioned|p387|||See also P388.||||||
26559|Fossil Cliff Formation|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
26559|Fossil Cliff Formation|36890|3|Fully described|p232|||Formerly Fossil Cliff Beds||||||
26559|Fossil Cliff Formation|37104|6|Mentioned|Fig.3|||||||||
26559|Fossil Cliff Formation|38917|6|Mentioned|p169|||||||||
26559|Fossil Cliff Formation|41053|6|Mentioned|p98|||||||||
26559|Fossil Cliff Formation|41514|4|Described|p62|||Although this unit onformably overlies and interfingers with Holmwood Shale, it  "is best regarded as a member of the Holmwood Shale" as concluded by Playford et al (1976). Conformably overlain by High Cliff Sandstone. Geol. prov: Perth Basin.||||||18-AUG-08
26559|Fossil Cliff Formation|42309|6|Mentioned|p245|||||||||
26559|Fossil Cliff Formation|42654|6|Mentioned|p14|||||||||
26559|Fossil Cliff Formation|43474|14|Not recorded|p55,71|||||||||
26559|Fossil Cliff Formation|43737|6|Mentioned|p2||Sakmarian|||||||
26559|Fossil Cliff Formation|43879|14|Not recorded|p254||Permian|Irwin Basin||||||
26559|Fossil Cliff Formation|44219|14|Not recorded|p31||Sakmarian|||||||
26559|Fossil Cliff Formation|44237|14|Not recorded|Fig.2||Permian|||||||
26559|Fossil Cliff Formation|44994|6|Mentioned|Fig.7|||Perm. Correlation||||||
26559|Fossil Cliff Formation|45001|14|Not recorded|p7|Artinskian|Sakmarian|||||||
26559|Fossil Cliff Formation|45016|14|Not recorded|p.55,72|||||||||
26559|Fossil Cliff Formation|46849|6|Mentioned|Fig. 6|||||||||
26559|Fossil Cliff Formation|48615|14|Not recorded|p.3,5, Fig.2,5,Pl.1.|||(H50-9).||||||
26559|Fossil Cliff Formation|48831|14|Not recorded|p.10,12,18,39,41|||||||||
26559|Fossil Cliff Formation|48848|14|Not recorded|p.90|||On many pages. p.39,42-3,60-1,66,74-87,89,90,102.||||||
26559|Fossil Cliff Formation|48857|14|Not recorded|p.18|||||||||
26559|Fossil Cliff Formation|60295|5|Briefly described|p130|||Geological Province: Perth Basin||||||
26559|Fossil Cliff Formation|61811|6|Mentioned|p36, p38.|Permian|Permian|Of Clarke et al. (1951); redefined to Member status after Johnson et al. (1954) and Playford et al. (1976) noted the unit was thin, lenticular and difficult to map. ||||||
26559|Fossil Cliff Formation|64635|6|Mentioned|p18|||Of Clarke et al.(1951); subsequently Fossil Cliff Member of Holmwood Shale (Johnson et al., 1954; Playford et al., 1976).||||||
26559|Fossil Cliff Formation|64974|6|Mentioned|p143, p144 Fig. 3|Sakmarian|Sakmarian|Geological Province: Perth Basin.||||||24-JUN-09
26559|Fossil Cliff Formation|69182|6|Mentioned|Ch2 p34-p41|||||||||
35636|Fossil Cliff Limestone Member|23279|6|Mentioned|p12|||||||||
35636|Fossil Cliff Limestone Member|44144|6|Mentioned|p508 Tb.4-21, p511 Fig.4-147|Sakmarian|Sakmarian|||Holmwood Shale|||Fossiliferous limestone.|
83945|Four Mile Hill dyke|70482|6|Mentioned|p319|Archean|Archean|This age determination is for a disturbance event, not time of emplacement.|2613 Ma (Nelson, 1995).||||Felsic porphyritic dyke.|
83352|Four Mile porphyry|73391|6|Mentioned|p26||||2613 +/- 11 Ma.|||||
38977|Frank River Schist|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
81591|Fraser Gabbro|72059|5|Briefly described|p57|Mesoproterozoic|Mesoproterozoic|Geological province: Fraser Zone, Albany-Fraser Orogen. Local name for voluminous metagabbroic rocks that dominate the Fraser Zone.||||||03-SEP-19
81591|Fraser Gabbro|73597|5|Briefly described|p1186, 1192 Fig.10|Mesoproterozoic|Mesoproterozoic|Fraser Zone, Albany-Fraser Orogen. Hosts sulfide-bearing mafic-ultramafic bodies including the 1304 +/- 22 Ma Nova-Bollinger Ni-Cu-Co deposit. Deformation and granulite-facies metamorphism was synchronous with magmatism. Trace element data graphed, discussed. Also referred to, throughout the text, informally as Fraser gabbro (p1182, 1186, 1191, 1193), Fraser gabbros (p1177, 1179, 1191-1192) and Fraser gabbro suite (p1177, 1192).|1305-1290 Ma.||||An extensive regional sheeted sill complex. Ranges from completely retextured mafic granulites to intrusions mostly retaining primary igneous cumulate textures.|
70463|Fraser Range gneiss|62093|6|Mentioned|p229|||Informal name. Geological Province: Albany-Fraser orogen.||||||
35349|Fraser River Limestone""|22776|6|Mentioned|p21|||Equivalent to Jarlemai Siltstone.||||||
80381|Fraser Suite|71169|5|Briefly described|p80|Ectasian|Ectasian|Intruded during Albany Fraser Orogen, stage 1. Deposited within a convergent plate margin setting [?]; magmatism during later extension (relaxation/delamination).|1305-1290 Ma||||Mafic intrusive rocks.|07-FEB-18
75965|Fraser dyke swarm|24165|5|Briefly described|p13, Plate 1|||Associated with the Albany-Fraser Orogeny.|c.1200 Ma.||||Dolerite dyke (interpreted from aeromagnetic data).|
75965|Fraser dyke swarm|64161|6|Mentioned|p580, p585 Fig.7|Ectasian|Ectasian|Interpreted by Wingate et al. (2000) to have intruded during an extensional episode between compressional events in the Albany-Fraser Orogeny.|1220-1200 Ma.|||Intrudes Stirling Range Formation.|Dolerite.|21-MAR-12
75965|Fraser dyke swarm|70017|6|Mentioned|p223-224|Mesoproterozoic|Mesoproterozoic|Part of the Marnda Moorn Large Igneous Province, in SE Yilgarn Craton. Paleomagnetic directions are relatively close to those of the Widgiemooltha dyke swarm (angular difference is 28 degrees).|c.1210 Ma.|||||
75965|Fraser dyke swarm|70085|6|Mentioned|p234 Fig.1|||Yilgarn Craton.||||||
75945|Fraser dykes|65368|5|Briefly described|p13|Ectasian|Ectasian|1212 Ma (Pisarevsky et al. 2003).||||||19-MAR-12
75945|Fraser dykes|68186|6|Mentioned|p30|||Informal name for NE-trending dykes in the eastern Albany-Fraser Orogen and southeastern Yilgarn Craton. Included in the Gnowangerup-Fraser Dyke Suite.||||||
75945|Fraser dykes|68471|6|Mentioned|p13, 15|||||||||
42467|Fred's Flow komatiitic basalt|60696|5|Briefly described|p341, p344|Archean|Archean|Informal name.||||||07-NOV-08
41302|Frere Formation, upper|50188|6|Mentioned|p8|||Informal - see Frere Formation.||||||16-JUL-08
41213|Frere formation|50223|6|Mentioned|p346|||Informal - see Frere Formation.||||||
41203|Frere granular iron-formation|50222|6|Mentioned|p328|||Informal - see Frere Formation.||||||
32741|Frezier Formation|24110|5|Briefly described|Plate 1|Cretaceous|Jurassic|Geological Province: Pilbara Craton||||||
32741|Frezier Formation|44998|14|Not recorded|p.119|||||||||
32741|Frezier Formation|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv|||Of Northern Carnarvon and Canning basins.||||Underlain by Callawa Formation.||
25916|Friendly Creek Formation|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
25916|Friendly Creek Formation|34829|6|Mentioned|Fig.2|||||||||
25916|Friendly Creek Formation|37373|6|Mentioned|p93|||||||||
25916|Friendly Creek Formation|39697|6|Mentioned|p92|||||||||
25916|Friendly Creek Formation|44150|6|Mentioned|p133 Tb.2-16|||Of Fitton et al. (1975). Obsolete; subsequently divided into North Star and Mount Ada Basalts, and McPhee and Duffer Formations.||||||
24992|Frigate Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p216, p217|Tithonian|Oxfordian|Of Mory, 1988. In figure, Fm = Formation. Geological Province: Bonaparte Basin. Consists of siltstones, shales and claystones with a uppermost carbonate unit.||||||01-MAR-10
24992|Frigate Formation|23376|4|Described|p229 Fig.2;p240,244|Kimmeridgian|Oxfordian|Of Bonaparte Basin.||||||19-SEP-06
24992|Frigate Formation|24234|5|Briefly described|p287 Fig.3|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin.||||||
24992|Frigate Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin.||||||
24992|Frigate Formation|41532|4|Described|p305|||||||||
24992|Frigate Formation|61548|6|Mentioned|p480 Fig.3|Late Jurassic|Middle Jurassic|Northern Bonaparte Basin. Part of regional play interval J50.||||||05-APR-22
24992|Frigate Formation|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Middle Jurassic|Age: ~160-~150Ma. Geological Province: Arafura and Money Shoals Basin.||||||01-MAR-10
24992|Frigate Formation|64689|5|Briefly described|p7 Fig.6 |Late Jurassic|Late Jurassic|||||||
24992|Frigate Formation|64696|6|Mentioned|p125-127, p131, p134, p138, p140 |Oxfordian|Oxfordian|See also reference to Frigate Shale (p134). Deep-marine basin fill following fault-controlled subsidence. Source rock.||||Interfingers with Lower Vulcan Formation.|Thick shale unit; anoxic shales in basal 20-30 m formed excellent source rocks.|
24992|Frigate Formation|68135|6|Mentioned|p61|||Northern Bonaparte Basin.||||||14-SEP-17
24992|Frigate Formation|68223|6|Mentioned|p178 Fig.3|Kimmeridgian|Oxfordian|||||||
24992|Frigate Formation|69653|6|Mentioned|p26-27, 50|||See also references to Frigate Shale (p1, 6, 8, 10, p13 Fig.2.4, p15, 37, 39, 41-43, 45, 47-49, 51, 53, 59, 63, 68, 73-74, 76).||||||
24992|Frigate Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||||
24992|Frigate Formation|70061|5|Briefly described|Regional geology; p7. Sahul: p1-2|||Oil-prone, syn-rift deposition was controlled by E-trending faulting due to Oxfordian-Kimmeridgian tectonism. Proven source rock in Sahul Syncline.||||||12-JUL-16
79250|Frigate Shale, Lower|69673|6|Mentioned|p173|||||Flamingo Group||||
79250|Frigate Shale, Lower|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin. Part of regional play interval J40.||||||05-APR-22
79250|Frigate Shale, Lower|70061|5|Briefly described|Petrel Sub-basin Fig.2|Late Jurassic|Late Jurassic|See also Regional geology: Figs.6-7. Sahul: Fig.2.||Flamingo Group.||Overlies Elang Formation. Is overlain by Upper Frigate Shale.||12-JUL-16
79251|Frigate Shale, Upper|70061|5|Briefly described|Petrel Sub-basin Fig.2|Late Jurassic|Late Jurassic|See also Regional geology: Figs.6-7. Sahul: Fig.2.||Flamingo Group.||Overlies Lower Frigate Shale. Is overlain by Sandpiper Sandstone.||12-JUL-16
23604|Gabanintha Formation|22774|4|Described|p571, Fig.2 p573|||Age of unit 2957-2951 Ma. See also p573||||||
23604|Gabanintha Formation|23135|5|Briefly described|p279 Fig.1|||||||||
23604|Gabanintha Formation|23146|5|Briefly described|p149|||of Luke Creek Group.||||||
23604|Gabanintha Formation|23148|4|Described|p112 Table.2|||||||||
23604|Gabanintha Formation|23922|5|Briefly described|p1234|Archean|Archean|Geological Province: Murchison-Southern Cross Terrane, Yilgarn Craton.  Parent: Luke Creek Group.||||||07-NOV-08
23604|Gabanintha Formation|24160|6|Mentioned|p112.|||||Unit in Luke Creek Group.||||
23604|Gabanintha Formation|24295|5|Briefly described|p1229|||Of the Luke Creek Group. Geological Province: Murchison province, Yilgarn Craton.||||||
23604|Gabanintha Formation|42533|3|Fully described|p26, p45|||Age approx. 3000Ma. Name reserved.||||||
23604|Gabanintha Formation|43769|5|Briefly described|p865|||||||||
23604|Gabanintha Formation|44149|5|Briefly described|p32, p35 fig 2-30, p36-37, p42 Fig.2-43|Archean|Archean|See also p43 Fig.2-44, p44 Fig.2-46, p45 Fig.2-48, p47, p57 Fig.2-71, p58 Fig.2-72,-73. Extends over whole Murchison Province; had the characteristics of a lava plain erupted in deep water. Upper portion thought to be remnants of stratovolcanoes. Appears as Gabanintha Complex in Fig.2-125.|~3000|Luke Creek Group||Overlain by Windaning Formation.|Thin basal basalt, overlain by an ultramafic intrusive-volcanic complex, then a thick interlayered high-Mg basalt and tholeiitic basalt succession, overlain by a mixture of mafic and felsic volcanics and derived sediments.|
23604|Gabanintha Formation|64891|6|Mentioned|p36|||||||||07-FEB-11
23604|Gabanintha Formation|65268|5|Briefly described|p6 fig 4, p6|||SHRIMP U-Pb zircon ages from rhyolitic to dacitic rocks.|2960 +/- 6 Ma to 2945 +/- 4 Ma (Wang et al. 1998)|Luke Creek Group|||Interlayered high-Mg and tholeiitic basalt.|
23604|Gabanintha Formation|68107|6|Mentioned|p619 Fig.8|Mesoarchean|Mesoarchean|Youanmi Terrane.||||||
23604|Gabanintha Formation|69153|6|Mentioned|Rocks.csv||||||||Sample descriptions include: dunite and olivine gabbronorite; igneous ultra/mafic intrusive|
23604|Gabanintha Formation|69267|5|Briefly described|p652, 654|||Murchison Province, Yilgarn Craton. Forms a substantial part of every greenstone belt in the Province.||Luke Creek Group.||Overlies Golconda Formation. Is overlain by Windanning Formation.|Ultramafic, mafic and felsic volcanic rocks and sediments.|
23604|Gabanintha Formation|69404|6|Mentioned|p4 Fig.4|Mesoarchean|Mesoarchean|Youanmi Terrane. |c. 2950 Ma|||||
76062|Gabanintha gabbro|66195|5|Briefly described|p611 Fig.9, p605|Mesoarchean|Mesoarchean|Informal name for Lady Alma Igneous Complex gabbro sample dated by Wang (1998).  Age may come from inherited granitic source.|2821+/-5 Ma.|||?intrudes the Norie Group.||13-MAR-12
76062|Gabanintha gabbro|70020|6|Mentioned|p118|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton.||||||
76062|Gabanintha gabbro|71168|5|Briefly described|p7|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||||||
78618|Gabanintha metagabbro|68561|5|Briefly described|GEOCHRON files|||Murchison Domain, Youanmi Terrane.  U-Pb zircon age: 2821 +/- 5 Ma. See geochron file 194747.1.pdf.||Lady Alma Igneous Complex||||
78618|Gabanintha metagabbro|71269|5|Briefly described|194747.1|||Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Of Lady Alma Igneous Complex. Wang 1998 provided U-Pb age of 2821+\-5 Ma.||Unit of Meeline Suite.||||
36115|Gabanintha rhyolite|23441|6|Mentioned|p156|||||||||
40544|Gabannintha Formation|23955|4|Described|p1240|||Of the Luke Creek Group. Geological Province: Murchison province, Yilgarn Craton.||||||
30143|Gage Member|43096|5|Briefly described|Fig.2|||of South Perth Shale.||||||
78774|Gairdner dyke swarm|63562|6|Mentioned|p337|||Plume-related magmatism.|c. 800 Ma|||||06-DEC-17
78774|Gairdner dyke swarm|69437|5|Briefly described|p22:3, 12|||Of the Gairdner Large Igneous Province.  Intrudes Supersequence 1 in the Officer and Amadeus Basins.|c.825 Ma.|||Correlated with Amata Dolerite.||12-JUL-16
78774|Gairdner dyke swarm|69873|5|Briefly described|p73, p82|||Possible equivalent of Tayatea Dyke Swarm in Tasmania. Appears as Gairdner Dyke Swarm on p82. A similar age of 824 +/- 4 Ma is from Glikson et al., (1996).|827 +/- 6 Ma (Wingate et al., 1998).|||||
78774|Gairdner dyke swarm|70744|5|Briefly described|p939|||Magmatism was coeval with breakup of Rodinia (860-570 Ma).|827 Ma (Wingate et al., 1998).|||||
78774|Gairdner dyke swarm|72259|6|Mentioned|p1, p9|||[Written as Gairdner-Amata dyke swarm and Gairdner-Amata Dyke (G-A) dyke swarm].||||||
78774|Gairdner dyke swarm|72488|6|Mentioned|p16||||~825 Ma.|||||
78774|Gairdner dyke swarm|73166|6|Mentioned|p644|Neoproterozoic|Neoproterozoic|Gawler Craton. Intrudes the Olympic Cu-Au Province.|0.83 Ga|||||
77411|Gairdner dykes|65135|4|Described|p17|Cryogenian|Cryogenian|Informal name. Medium-grained intergranular to subophitic dolerite, but shows polygonal granoblastic textures where recrystallised. Mostly northwest- to north-trending. Zircon U-Pb age of 824 +/- 4 Ma in WA and baddeleyite age of 827 +/- 6 Ma in the Stuart Shelf (Wingate et al., 1998). Linked with the Amata dykes on the basis of similar ages and chemistry (Glikson et al., 1996). Cross-cut Kullal dykes and Giles intrusions.||||||
77411|Gairdner dykes|65693|5|Briefly described|p12.|||Evidently a casual form of referring to dykes of Gairdner Dolerite.|825 Ma.|||||
77411|Gairdner dykes|67128|5|Briefly described|p8|||Musgrave Province.|c.800 Ma.||||Mafic dykes.|
77411|Gairdner dykes|70083|6|Mentioned|p207|||Intrudes much of the Musgrave Inlier.|c.800 Ma.||||Dolerite.|
77411|Gairdner dykes|70738|6|Mentioned|p189, 191|||Gawler Craton. See also references to the Gairdner Dyke Swarm (p186-187, 189, 196 Fig.10).|c.820 Ma.|||||
77411|Gairdner dykes|72725|6|Mentioned|p6-7|||[Variation on Gairdner Dolerite? Written as Gairdner dyke anomalies and Gairdner dykes.]||||||
77411|Gairdner dykes|73086|6|Mentioned|p9|||Gawler Craton.||||Correlates to Amata Dolerite.||
40766|Galah monzogranite|24494|6|Mentioned|p21|||Informal - see Galah Monzogranite.||||||
69656|Gamma Formation|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Overlain by, underlain by and interfingers with Revenge Formation. Age: 17.5-14.5Ma. Thickness: 2m. Geological region: Norseman region. ||||||
74958|Gamma Island Dolomite|64646|6|Mentioned|p23 Fig. 3|Miocene|Miocene|Geological Province: Yilgarn Craton.||||||
74958|Gamma Island Dolomite|69598|6|Mentioned|p9, p10|Middle Miocene|Early Miocene|||Redmine Group|||Interbedded lacustrine carbonates.|
37214|Gamma Island formation|23989|5|Briefly described|p54 Fig. 46|Cenozoic|Cenozoic|Informal name. Geological Province: Yilgarn Craton||||||19-NOV-08
27778|Gap Creek Dolomite|30983|4|Described|p73|||||||||
27778|Gap Creek Dolomite|33731|6|Mentioned|p614|||Trilobites.||||||
27778|Gap Creek Dolomite|33738|6|Mentioned|p55|||||||||
27778|Gap Creek Dolomite|35119|6|Mentioned|p448, p461|||See also p461. Replaced by Gap Creek Formation.||||||21-APR-17
27778|Gap Creek Dolomite|41055|6|Mentioned|Fig.1|||||||||
27778|Gap Creek Dolomite|43563|6|Mentioned|p4|||||||||
27778|Gap Creek Dolomite|43803|6|Mentioned|p65|||superseded||||||
27778|Gap Creek Dolomite|44998|14|Not recorded|p22,40|||||||||
27778|Gap Creek Dolomite|45153|6|Mentioned|App.1-15|||Now named Gap Creek Formation||||||
27778|Gap Creek Dolomite|48831|14|Not recorded|p.82|||||||||
68830|Gap Creek Formation, lower|50089|6|Mentioned|p427|Ordovician|Ordovician|Informal - see Gap Creek Formation.||||||
33906|Garden Creek adamellite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3007 Ma||||||07-NOV-08
80253|Garden Monzogranite|71311|5|Briefly described|p797|||Cue-Mount Magnet area. Post-tectonic.|2.62 Ga.|||||
69966|Gascoyne Complex, Northern|50217|6|Mentioned|p222|||Informal - see Gascoyne Complex.||||||
69966|Gascoyne Complex, Northern|50219|6|Mentioned|p258 Fig. 1|||Informal - see Gascoyne Complex.||||||07-FEB-11
69966|Gascoyne Complex, Northern|50228|5|Briefly described|p491 Fig.10|||Informal - see Gascoyne Complex||||||
69966|Gascoyne Complex, Northern|64777|6|Mentioned|p1 Fig.2, p6-8|Palaeoproterozoic|Palaeoproterozoic|Informal reference to northern part of the Gascoyne Complex. Presented as Northern Gascoyne Complex in map figure and graphs.||||||
41204|Gascoyne Complex, Southern|50217|5|Briefly described|p220, p221 Fig.1|||Informal - see Gascoyne Complex. includes 2550 Ma gneissic granites.||||||
41204|Gascoyne Complex, Southern|50219|6|Mentioned|p258 Fig. 1|||Informal - see Gascoyne Complex.||||||07-FEB-11
41204|Gascoyne Complex, Southern|50222|6|Mentioned|p333 Tb. 2|||Informal reference to southern part of the Gascoyne Complex.||||||
41204|Gascoyne Complex, Southern|50228|5|Briefly described|p491 Fig.10|||Informal - see Gascoyne Complex||||||
41204|Gascoyne Complex, Southern|64777|6|Mentioned|p1 Fig.2, p6-8 |Palaeoproterozoic|Palaeoproterozoic|Informal reference to southern part of the Gascoyne Complex. Presented as Southern Gascoyne Complex in map figure and graphs.||||||
41204|Gascoyne Complex, Southern|66106|6|Mentioned|p44|||Affected by numerous Orogenies, granite intrusions and dolerite dyke swarms.||||||
42479|Gascoyne Complex, northern|50216|6|Mentioned|p211 Fig.4|||Informal - see Gascoyne Complex.||||||
41205|Gascoyne Complex, southern|24332|5|Briefly described|p144|||Refers to the southern section of the Gascoyne Complex - informal name.||||||24-JAN-06
41205|Gascoyne Complex, southern|50216|6|Mentioned|p203|||Informal - see Gascoyne Complex.||||||
41205|Gascoyne Complex, southern|50218|6|Mentioned|p250|||Informal - see Gascoyne Complex.||||||07-FEB-11
41205|Gascoyne Complex, southern|50219|6|Mentioned|p259|||Informal - see Gascoyne Complex.||||||07-FEB-11
41205|Gascoyne Complex, southern|50220|5|Briefly described|p280|||Not a formal straigraphic name. Southern part of the Gascoyne Complex, as a structural unit, is now redefined as Glenburgh Terrane - consisting of metamorphosed and variably deformed tonalite, granodiorite and monzogranite.||||||
41205|Gascoyne Complex, southern|50222|6|Mentioned|p333 Tb. 2, p335, 337|||Informal reference to southern part of the Gascoyne Complex.||||||22-JUN-04
40446|Gascoyne complex|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt. See also p855. Informal - see the Gascoyne Complex.||||||
40446|Gascoyne complex|50222|6|Mentioned|p331 Fig. 6|||Informal - see Gascoyne Complex.||||||
41229|Gascoyne granitoids|50226|6|Mentioned|p430 Fig. 7|||Informal reference to granitoid rocks of the Gascoyne Complex.||||||
40780|Gearle Sandstone|50085|5|Briefly described|p23 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
40780|Gearle Sandstone|61023|5|Briefly described|p27 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||11-APR-08
40780|Gearle Sandstone|62837|5|Briefly described|Stratigraphic columns|Turonian|Early Cretaceous|Overlies Windalia Radiolarite.  Age: ~110-90Ma. Geological Province: Northern Carnarvon Basin and Roebuck Basin.||||||07-NOV-06
40780|Gearle Sandstone|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
40079|Gearle Siltstone Formation|24205|6|Mentioned|p250 Fig. 6|||||||||
28567|Gearle Siltstone member|41172|6|Mentioned|p129|||||||||
40295|Gearle Siltstone""|23915|6|Mentioned|p539|Cenomanian|Albian|Informal-see Gearle Siltstone.||||||
74495|Gearle Siltstone, Lower|63950|5|Briefly described|p336 Fig. 4|Turonian|Albian|Overlies Windalia Radiolarite; underlies the upper section of Gearle Siltstone. Geological Province: northern Carnarvon Basin.||||||01-FEB-10
74495|Gearle Siltstone, Lower|67784|6|Mentioned|p26, p28 Tb.1, p30-34|||Carnarvon Basin.
||||||08-FEB-18
74495|Gearle Siltstone, Lower|68206|6|Mentioned|p30, 32|Albian|Albian|Carnarvon Basin. See also references to Gearle Siltstone (p29-30) and Gearle Siltstone, Upper (p30, 32-33).||||Overlies Windalia Radiolarite. Is overlain by Upper Gearle Siltstone.||
74495|Gearle Siltstone, Lower|69182|6|Mentioned|Ch3 p40, |Late Cretaceous|Late Cretaceous|Generally too shallow (less than 750m deep) to act as a suitable seal of carbon dioxide storage. ||||||
74495|Gearle Siltstone, Lower|69692|6|Mentioned|p4|Late Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||||Overlies Windalia Radiolarite. Is overlain by Upper Gearle Siltstone.||
40293|Gearle Siltstone, Upper|23915|5|Briefly described|p520 Fig. 3|Santonian|Turonian|Informal-see Beedagong Claystone.||||||
40293|Gearle Siltstone, Upper|63950|5|Briefly described|p336 Fig. 4|Santonian|Turonian|Overlies lower section of Gearle Siltstone. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
40293|Gearle Siltstone, Upper|67784|6|Mentioned|p26, p28 Tb.1, p30-34|Cenomanian|Albian |Carnarvon Basin.||||||08-FEB-18
40293|Gearle Siltstone, Upper|68206|6|Mentioned|p30, 32-33|Cenomanian|Albian|Carnarvon Basin. See also references to Gearle Siltstone (p29-30) and Gearle Siltstone, Lower (p30, 32).||||Overlies Lower Gearle Siltstone. Is overlain by Haycock Marl and Toolonga Calcilutite.||
40293|Gearle Siltstone, Upper|69692|6|Mentioned|p4|Late Cretaceous|Late Cretaceous|Northern Carnarvon Basin.||||Overlies Lower Gearle Siltstone. Is overlain by Toolonga Calcilutite.||
40292|Gearle Siltstone, lower""|23915|5|Briefly described|p539|Cretaceous|Cretaceous|Informal-see Gearle Siltstone.||||||
72891|Gearle Siltstone, upper|63068|6|Mentioned|p46|||Informal - see Gearle Siltstone. Often includes unrecognised Haycock Marl, which actually overlies this siltstone as a thin unit. Geological Province: Carnarvon Basin.||||||27-FEB-07
40294|Gearle Siltstone, upper""|23915|5|Briefly described|p539|Santonian|Turonian|Informal-see Beedagong Claystone.||||||
24999|Gearle siltstone|35333|6|Mentioned|p12|||||||||
32575|Gee Cee Slate|45543|4|Described|p.102||Archean|Unit of Woolyeenyer Group.||||||07-NOV-08
81303|Gemchapps monzogranite|70020|6|Mentioned|p122|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.||||||
38075|George River Volcanic Complex|23570|6|Mentioned|p73|||||||||
83377|Gibson-Honman formation|73391|4|Described|p194-195, 200, 244-245, 247, 285, 304|||See also p417, 419-420, 441-442, Appendices. Ora Banda Domain, Kalgoorlie Terrane. Called Gibson-Honman rock on p200. Appears as Gibson-Honman Formation on p285. Sub-marine lava dome complex. Incorporates felsic volcanic rocks at Gibson-Honman Rock, Lakewood dacitic volcanics, and Perkolilli rhyolitic volcanics.|~2679-2675 Ma.|Lower Black Flag Formation/Group.||Gradationally overlies (Upper) White Flag Formation. Is overlain unconformably by Gidji Lake formation (Upper Black Flag Formation).|Strongly weathered feldspar-phyric dacite.|
83379|Gidji Lake formation|73391|4|Described|vii-viii, 180, 194-195, 200, 244-245|||See also p247, 304, 417, 419-421, 441-443, Appendices. Fimiston area, Kambalda Domain, Kalgoorlie Terrane. Incorporates felsic volcaniclastic rocks at Gidji, Binduli Porphyry Conglomerate and Grave Dam Grit. This 2682 Ma crystallisation age is accompanied by an MDA of a felsic volcanic breccia clast of 2660 +/- 16 Ma. See Gidji Lake Formation.|2682 +/- 6 Ma. (SHRIMP: Tripp, 2019).|Upper Black Flag Group.|Binduli Porphyry Conglomerate, Grave Dam Grit.|Unconformably overlies Lakewood dacite (Gibson-Honman formation). Is overlain unconformably by Navajo sandstone. Correlated with Binduli Porphyry Conglomerate (Upper Black Flag Formation).|Coarse clastic sedimentary and volcanic rocks: includes felsic volcaniclastic rocks eg carbonate altered biotite-hornblende porphyry.|
83378|Gidji conglomerate|73391|6|Mentioned|p241, 244, 318, 416, Appendices.|||Kambalda area. Only capitalised on p416.|<2660 Ma.|||||27-JUN-22
40074|Gidley Granophyre complex|24541|6|Mentioned|p56|Paleoproterozoic|Neoarchean|Informal - see Gidley Granophyre.||||||07-NOV-08
77222|Gifford Complex|66299|6|Mentioned|p305.|||Named by Pearson et al. (1996); subsequently renamed Gifford Creek Carbonatite Complex (Pirajno et al. in prep. at time of this study) for lack of alkaline igneous rocks other than carbonatite. ||||||
79538|Gifford Creek Carbonatite Suite|69003|5|Briefly described|p4, p41, p43|||Northern Gascoyne Province, Capricorn Orogen. Intrusions occurred during the Mutherbukin Tectonic Event, and extensively fenitized the country rock to form abundant sodic amphibole and a variety of other alkaline minerals. Associated with REE-mineralised ironstone veins and dykes (described in some detail).|c.1300-c.1280 Ma.|||Intrudes Durlacher Supersuite.|Sills, dykes and veins of ferroan carbonatite, ironstone and hydrothermally altered rocks.|
79538|Gifford Creek Carbonatite Suite|71869|6|Mentioned|p4||||c. 1300 Ma|||||
41230|Gifford Creek Complex|22660|4|Described|p 300||Mesoproterozoic|Informal Name p299.  It is the largest area of alkali metasomatised rock currently recognised in Australia.||||||
41230|Gifford Creek Complex|50226|5|Briefly described|p418||Paleoproterozoic|Age: 1.68 Ga (Pearson et al, 1996).||||||07-NOV-08
41230|Gifford Creek Complex|64287|6|Mentioned|p32, p33|||Probably a structural term? See also Fig. 1.||||||07-FEB-11
41230|Gifford Creek Complex|64329|5|Briefly described|p15, p20, p27 Tb. 7|||Includes pyrochlore-bearing sills (Spider Hill sills), limonitic intrusions (Bald Hill intrusions) and fluidisation breccias forming the largest area of metasomatic rock currently recognised in Australia; also includes the Yangibana ironstones.||||||05-AUG-08
41230|Gifford Creek Complex|69080|6|Mentioned|p701|||Of Pearson (1996), Pearson and Taylor (1996), Pearson et al. (1996). Subsequently Gifford Creek Carbonatite Complex.||||||
79804|Gifford Creek Ferrocarbonatite Complex|69237|5|Briefly described|p1-17|||Pirajno and Gonzalez-Alvarez (2013). Formerly the Gifford Creek Carbonatite Complex (Pirajno et al., 2010) but renamed to recognise the preponderance of iron carbonate, in some cases exclusively. The authors do not accept the name Gifford Creek Ferrocarbonatite Suite (Johnson, 2013), because the lithologies show irregular and complex structural and compositional features. Gascoyne Province. Occupies c.700 km2.||||Intrudes Pimbyana, Yangibana Granites and Bangemall Supergroup.|A carbonatite complex (rocks with >50% carbonates, fluoroapatite, nepheline and other feldspathoids), characterised by ferrocarbonatite sills, dykes and veins, that are surrounded by variably fenitised country rocks. Widespread iron oxide veins.|
79804|Gifford Creek Ferrocarbonatite Complex|69546|4|Described|p100-101,104-105,107,113,115,117|Stenian|Stenian|Geological province: Gascoyne Province. Formerly named Gifford Creek Carbonatite Complex, and renamed as a ferrocarbonatite complex as it was surrounded by fenetised country rock (Pirajno et al., 2010). Also previously called the Gifford Creek Igneous Complex. Commonly abbreviated in text as GFC. Ferrocarbonatites are associated with complex and irregularly distributed zones of fenitic alteration. Ferrocarbonatite sills and dykes form a NW-trending belt in the SW part of GFC, turning into a northern WNW-trending belt of ironstone veins and carbonatite swarms (termed Bald Hill Lineament). the GFC was emplaced along Lyons River Fault (deep crustal structure). In-situ U-Pb dating of apatite grains by LA-ICP-MS from a sample of ferrocarbonatite, yielding an average age of 1075+\-35 Ma, while monazite grains from fenitic rocks associated with the ironstone veins returned a concordia age of 1050+\-24 Ma. Apatite age suggests an association with the Warakurna LIP, while monazite age might record strike-slip movements along Lyons River Fault.||||Intruded into Pimbyana Granite, Yangibana Granite, Durlacher Supersuite and metasedimentary rocks of the Pooranoo Metamorphics.|Sills and dykes (carbonate-rich matrix, containing fluoroapatite, celestite, bastnaesite, phlogopite, barite and monazite), and veins of ferrocarbonatite (ankerite, dolomite, magnetite, Fe-Ti oxides, and arfvedsonite-riebeckite).|05-JUL-19
79804|Gifford Creek Ferrocarbonatite Complex|71210|6|Mentioned|p135|||West Australian Craton.||||||
79804|Gifford Creek Ferrocarbonatite Complex|74493|6|Mentioned|p13|||Name used by Pirajno et al., (2014) for the Lyons River Sills due to high bulk Fe contents resulting from significant magnetite contents.||||||
78904|Gifford Creek Ferrocarbonatite Suite|69237|6|Mentioned|p3|||Johnson (2013). The authors prefer the term Complex over Suite, as the lithologies show irregular and complex structural and compositional features.||||||
78904|Gifford Creek Ferrocarbonatite Suite|69387|5|Briefly described|p37-38, p40, p52, p63, p66|Proterozoic|Proterozoic|Cited as an example of the variety of mineralisation styles in the Gascoyne Province; in this case, carbonatite-related REEs, at e.g. the Yangibana prospect (described). U-Th-Pb SHRIMP monazite magmatic age.|c.1300 Ma (Johnson, 2013).||||A high-level alkaline complex.|
78904|Gifford Creek Ferrocarbonatite Suite|69596|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Gascoyne Province.||||||
78904|Gifford Creek Ferrocarbonatite Suite|70795|4|Described|100k_interpgeol_lut.csv|Neoproterozoic|Paleoproterozoic|Also 500k_interpgeol_lut.csv, West Australian Craton|1619-570 Ma||||Hematite-magnetite veins, locally altered to massive goethite; fenite alteration comprises variable amounts of k-feldspar, albite, sodic amphibole and cancrinite. Ferroan carbonatite; sills and dykes of Fe-carbonate, phlogopite and sodic amphibole.|
78904|Gifford Creek Ferrocarbonatite Suite|70814|6|Mentioned|p49|||||||||
75935|Gifford Creek Igneous Complex|64872|6|Mentioned|p23|Proterozoic|Proterozoic|Gascoyne Complex. Mineralisation styles include carbonatite-related rare earth elements including uranium. Multiple reworking episodes mean controls on mineralisation are poorly understood.||||||16-MAR-12
75935|Gifford Creek Igneous Complex|69166|5|Briefly described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||||Ferroan carbonatite; sills and dykes of Fe-carbonate, phlogopite and sodic amphibole and variable amounts of quartz|
75935|Gifford Creek Igneous Complex|69237|5|Briefly described|p2-3|||Pearson (1966), Pearson et al. (1996). Later renamed the Gifford Creek Carbonatite Complex (Pirajno et al. (2010) and subsequently the Gifford Creek Ferrocarbonatite Complex.|||||High-level alkaline intrusions: ultrabasics, and  a younger phase of dykes and sills of carbonatitic affinity.|
83190|Gifford Creek carbonatite|73056|6|Mentioned|p298|Ectasian|Ectasian|Capricorn Orogen, Edmund Basin.|ca. 1360 Ma|||||
83189|Gifford Creek carbonatite complex|73056|6|Mentioned|p301|Ectasian|Ectasian|Edmund Basin.|ca. 1360 Ma|||||
41231|Gifford Creek complex|50226|6|Mentioned|p427|||Informal - see Gifford Creek Complex.||||||
35900|Giles Complex gabbro -Po|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Gabbro, norite, troctolite, anorthosite and ultramafic rocks - generally well banded.||||||
35900|Giles Complex gabbro -Po|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Gabbro, norite, troctolite, anorthositic gabbro, generally well banded; includes minor ultramafic rocks and acid differentiates.||||||
35900|Giles Complex gabbro -Po|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Gabbro, troctolite, anorthositic gabbro - generally well banded.||||||
75233|Giles Intrusions|64745|5|Briefly described|p376|||Informal name. Alcurra Dolerite may represent feeder systems to Giles Intrusions. See Giles Complex.||||||
80999|Giles Suite 2|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1078-1074 Ma (inferred)|Unit of Warakurna Supersuite.|||Amphibolite, gabbro and metagabbro, metagabbronorite, leucogabbronorite.|
80999|Giles Suite 2|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Informal subdivision of Giles Suite. Of Warakurna Large Igneous Province. Age inferred: 1078- 1074 Ma.||Warakurna Supersuite|Includes one unnamed subunit.||Mafic intrusive rock; massive or weakly layered; locally mingled with leucogranite.  Moderately to strongly foliated amphibolite after fine- to medium-grained gabbro; strongly epidotized , cut by abundant quartz + pegmatite veins; locally mylonitic.|
74665|Giles intrusions|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Warakurna Supersuite. SHRIMP Ages from Sun et al, 1996 AGSO Research Newsletter 24 p13-15.||||||11-SEP-08
74665|Giles intrusions|65135|4|Described|p4 Fig.3, p14||Stenian|Informal name. Layered mafic-ultramafic intrusives. Forms the west-northwest spine of the west Musgrave Complex. Age is poorly constrained. Maximum age of ~1170 Ma. Reaches a maximum thickness of ~10 km in the Jameson area. Granites related to the Giles Event and temporally associated with the massive gabbros show strongly developed A-type compositional characteristics (Sheraton and Sun, 1995).||||||
74665|Giles intrusions|67128|5|Briefly described|p6-7, p10-11, p15, p18-21|||Another name for Giles Complex (p5 Fig.4). Intruded the boundary between the Tjuni Purlka Tectonic and Mamutjarra Zones. Initial volume nearly 50,000 km3. Forms prominent hills in the Musgrave Ranges. Also appears as Giles Intrusions (p7). Significant economic potential for Ni-Cu and PGE mineralisation.|c.1120-1078 Ma.|||Intrudes or overlies Mummawarrawarra Basalt.|Giant, layered mafic-ultramafic intrusions.|
74665|Giles intrusions|69003|4|Described|p37, p50-52|Mesoproterozoic|Mesoproterozoic|W Musgrave Province. Associated with the Giles Event. Cumulative thickness c.10km, but likely was a single large intrusion 170km long, 25km wide and 10km thick, tectonically dismembered.||Warakurna Supersuite.|||Giant, layered mafic-ultramafic intrusions; mainly troctolite or gabbroic with minor peridotite.|
74665|Giles intrusions|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin.||||Overlain by Winburn granite or Mount Palgrave Group. Underalin by Kunmarnara Group.||
74665|Giles intrusions|73058|6|Mentioned|p768|Stenian|Stenian|Musgrave Province. Intruded boundary between Mamutjarra and Tjuni Purlka Tectonic Zones.|c. 1085-1040 Ma|Warakurna Supersuite|||Giant mafic-ultramafic bodies.|
74665|Giles intrusions|73437|6|Mentioned|p153|||Formed during Giles Event. See also Giles Suite p151.||Warakurna Supersuite|||Giant layered mafic-ultramafic intrusions.|
27156|Gindalbie Formation|23142|5|Briefly described|p202|||||||||
27156|Gindalbie Formation|29784|6|Mentioned|Table 1|||||||||
27156|Gindalbie Formation|30632|6|Mentioned|p230|||||||||
27156|Gindalbie Formation|30882|4|Described|p50|||Refers Stratigraphy||||||
27156|Gindalbie Formation|30900|6|Mentioned|p67|||On Table 1||||||
27156|Gindalbie Formation|30956|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27156|Gindalbie Formation|30965|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27156|Gindalbie Formation|31091|6|Mentioned|Fig. 2|||Also mention Fig. 3.||||||
27156|Gindalbie Formation|32268|6|Mentioned|Fig. 1|||||||||
27156|Gindalbie Formation|32269|6|Mentioned|p313|||||||||
27156|Gindalbie Formation|32694|6|Mentioned|p1093|||Refers Williams (1970)||||||
27156|Gindalbie Formation|33446|6|Mentioned|p15|||||||||
27156|Gindalbie Formation|33837|5|Briefly described|p165|||Archaean||||||
27156|Gindalbie Formation|33846|4|Described|p64|||Archean. Graded bedding.||||||13-NOV-08
27156|Gindalbie Formation|33847|2|Defined|p14|Archean|Archean|c 2660my. See also Table 4.||||||07-NOV-08
27156|Gindalbie Formation|33850|4|Described|Table 2|||Mention p7.||||||13-NOV-08
27156|Gindalbie Formation|36869|4|Described|p46|||||||||
27156|Gindalbie Formation|37004|6|Mentioned|p286|||See also Table 1.||||||
27156|Gindalbie Formation|38767|5|Briefly described|p91|||||||||
27156|Gindalbie Formation|40308|6|Mentioned|p82|||||||||
27156|Gindalbie Formation|41066|5|Briefly described|1 of 2 K15|||||||||
27156|Gindalbie Formation|41594|5|Briefly described|p41|||||||||
27156|Gindalbie Formation|42892|6|Mentioned|Table 3|||||||||
27156|Gindalbie Formation|44149|5|Briefly described|p91 Tb.2-9|Archean|Archean|Kurnalpi-Edjudina area, Eastern Goldfields Province.|||||Sandstone, felsic volcanics.|
27156|Gindalbie Formation|65834|6|Mentioned|p33|||Boorara Domain, Kalgoorlie Terrane. Hosts gold mineralisation in the Kanowna district (described in detail).||||Overlies Highway Ultramafics. Is correlated with Black Flag Group.||
27156|Gindalbie Formation|73391|6|Mentioned|Appendices.|||Williams (1969). Regional stratigraphic correlation chart of other workers.|||||Clastic sequence. Acid volcanic complexes.|
77547|Gindalbie Sequence|63980|4|Described|p63.|Archean|Archean|Same basement as Kurnalpi Sequence, implying they are fragments of same volcanic arc. HFSE-enriched granitoids and porphyries are associated  with bimodal and subalkaline volcanic complexes. Rifting of a marginal-arc system related to backarc spreading.|2694 +/- 4 Ma to 2676 +/- 5 Ma.||||Intermediate to silicic lava and high-level intrusions, coarse-grained volcanic breccias, subaqueously deposited volcanogenic sandstone; intruded by mafic to intermediate sills and dykes.|
77547|Gindalbie Sequence|66880|5|Briefly described|p9, pp26-27.|Archean|Archean|This new term refers to the supracrustal rocks of the Gindalbie Terrane. Facies and geochemistry consistent with intra-arc or arc-rift setting. Interpreted to overlie Kurnalpi Sequence andesites and basalts. Records early stages of arc rifting.|c.2695-c.2675 Ma.||||Bimodal basalt-rhyolite and calc-alkalic intermediate-silicic volcanic complexes, mafic sills and layered mafic complexes.|
77547|Gindalbie Sequence|66938|5|Briefly described|p195.|Archean|Archean|Gindalbie Terrane. Overlapped with the first stage of the Kalgoorlie Sequence. Different geochemical affinity indicates a different arc-fragment.|||||An arc-rift succession with coeval calc-alkalic andesite-dacite-rhyolite, and bimodal HFSE-enriched rhyolite-basalt, volcanoplutonic centres.|
77547|Gindalbie Sequence|67198|5|Briefly described|p7|Neoarchean|Neoarchean|Kurnalpi Terrane.|c.2.7 Ga.||||Coeval felsic and mafic volcanics, andesitic volcanic centres.|11-SEP-17
81123|Gindalbie volcanics|68289|6|Mentioned|p6 fig 5,|||Eastern Goldfields Superterrane.|c. 2692-2680 Ma|||||
39248|Gingin Chalk formation|24094|5|Briefly described|p267|Late Cretaceous|Late Cretaceous|Informal - see Gingin Chalk. White chalky limestone with glaucanite and beds of greensand in some areas. Lies disconformably on the Dandaragan Sandstone. Geological Province: Perth Basin.||||||16-MAR-05
42389|Giralian Stage""|23815|6|Mentioned|p301|||Superseded by the Giralia Calcarenite (Condon and others, 1956).||||||
38400|Glass Springs Formation|24017|5|Briefly described|p27|||Of the Salvation Group.||||||07-AUG-08
38400|Glass Springs Formation|62453|6|Mentioned|p16|||||||||
78672|Glen Herring Creek Sequence|60112|5|Briefly described|p108-109, p111-112, p117. ||||c.2756 Ma (Arndt et al., 1991).|Unit in Fortescue Group.|Includes Hardey Formation and Kylena Basalt.|Unconformably to disconformably overlies the Mount Roe Sequence. Is overlain unconformably by Pear Creek Sequence.||
34329|Glen Herring Shale Member|22717|6|Mentioned|P10|||||||||
75974|Glenayle Dolerites|64724|6|Mentioned|p48|Mesoproterozoic|Mesoproterozoic|~1066 Ma. Collier Basin?||||||
33998|Glengarry Formation|22558|6|Mentioned|p576||Proterozoic|||||||
24288|Glengarry Group|12099|5|Briefly described|p676, p678 Fig.4|||Included Peak Hill Metamorphics, Finlayson Sandstone, Maraloou Formation, Crispin Conglomerate, Juderina Formation, Johnson Cairn Shale, Doolgunna Formation, Karalundi Formation, Narracoota Volcanics, Thaduna Greywacke, Horseshoe Formation and Labouchere Formation (Gee, 1987). Constituent units are placed under other groups in this paper.|||Juderina Formation (Finlayson Sandstone Member), Johnson Cairn Shale, Doolgunna Formation, Thaduna Greywacke, Narracoota Volcanics and Maraloou Formation (Gee and Grey, 1993).|||04-MAR-13
24288|Glengarry Group|22478|6|Mentioned|p23||Paleoproterozoic|Nabberu Basin||||||07-NOV-08
24288|Glengarry Group|22816|6|Mentioned|p15 Fig.7|||||||||
24288|Glengarry Group|22940|6|Mentioned|p10|||Obselete - upgraded to Glengarry Basin (Gee and Gray, 1993)||||||
24288|Glengarry Group|23045|6|Mentioned|295|||Geol province Yilgarn Craton||||||
24288|Glengarry Group|23151|5|Briefly described|p63|||||||||
24288|Glengarry Group|23152|5|Briefly described|p71|||||||||
24288|Glengarry Group|23589|6|Mentioned|p20|||||||||
24288|Glengarry Group|23593|5|Briefly described|p1|||||||||
24288|Glengarry Group|23723|5|Briefly described|p1|||Geological Province: Nabberu Basin.||||||
24288|Glengarry Group|23744|5|Briefly described|p1|||Replaced by Yerrida, Bryah and Padbury Groups. Geological Province: Yilgarn Craton.||||||
24288|Glengarry Group|23747|5|Briefly described|p1|||Geological Province: Glengarry Basin.||||||
24288|Glengarry Group|23749|5|Briefly described|p14|||Now divided into Yerrida and Bryah Groups.||||||
24288|Glengarry Group|23798|6|Mentioned|p2|||Geological Province: Yilgarn Craton.||||||
24288|Glengarry Group|35975|2|Defined|p100|Proterozoic|Proterozoic|||||||
24288|Glengarry Group|37299|6|Mentioned|Fig.1|||||||||
24288|Glengarry Group|37460|3|Fully described|p143|||||||||
24288|Glengarry Group|38243|6|Mentioned|Fig.2|||||||||
24288|Glengarry Group|38495|4|Described|p31|||||||||
24288|Glengarry Group|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|38880|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|38994|4|Described|p25|||||||||22-DEC-09
24288|Glengarry Group|39894|6|Mentioned|p48|||||||||
24288|Glengarry Group|40089|6|Mentioned|p4|||See also P207||||||
24288|Glengarry Group|40105|6|Mentioned|Fig.3|||||||||
24288|Glengarry Group|40297|4|Described|p109|||||||||
24288|Glengarry Group|40356|6|Mentioned|p16|||||||||
24288|Glengarry Group|40357|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24288|Glengarry Group|40937|3|Fully described|p28|||Mention P55||||||
24288|Glengarry Group|40938|4|Described|p10|||Mention P4||||||
24288|Glengarry Group|40989|4|Described|p15|||||||||
24288|Glengarry Group|41635|6|Mentioned|p18|||||||||
24288|Glengarry Group|41846|6|Mentioned|p94|||||||||
24288|Glengarry Group|41991|6|Mentioned|Fig.2A P128|||||||||
24288|Glengarry Group|42148|6|Mentioned|p698|||||||||
24288|Glengarry Group|42260|6|Mentioned|p9|||||||||
24288|Glengarry Group|42579|5|Briefly described|Table 2 P11|||||||||
24288|Glengarry Group|42730|5|Briefly described|p15|||||||||
24288|Glengarry Group|43069|1|Redefined|p29|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
24288|Glengarry Group|43595|5|Briefly described|p75,219,343,346||Paleoproterozoic|Deposition 2.2-1.8 Ga ago. Age: 1.8-2.2 Ga||||||07-NOV-08
24288|Glengarry Group|44111|6|Mentioned|p.56, Fig. 1|||||||||
24288|Glengarry Group|44149|6|Mentioned|p62 Tb.2-5|Archean|Archean|||||||
24288|Glengarry Group|49893|5|Briefly described|p8|Proterozoic|Proterozoic|Now included in the Yerrida and Bryah Groups.||||||
24288|Glengarry Group|49896|5|Briefly described|p2 Tb. 1|||Originally defined by Gee (1979a). Now superseded by Yerrida and Bryah Groups. Interpreted as a siliciclastic-dominated shelf succession. Age: 2.0-1.8Ga. See also p3 Tb. 2.||||||
24288|Glengarry Group|60460|6|Mentioned|p62|||||||||
24288|Glengarry Group|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|Sedimentary rocks, mafic sills and dykes.||||||07-FEB-11
24288|Glengarry Group|62289|5|Briefly described|p1-2, p4|Palaeoproterozoic|Palaeoproterozoic|Glengarry Basin defined by Gee and Grey (1993); divided into Bryah, Padbury, and Yerrida Groups by Pirajno and Adamides (2000).||||||
24288|Glengarry Group|64384|5|Briefly described|p77, p78 Tb. 78|||Incl: Juderina Fm., Johnson Cairn Shale, Doolgunna Fm., Karalundi Fm., Narracoota Volcanics, Thadunna Greywacke, Horseshoe+Labouchere Fms. Thick "greywacke-type" seds.(Gee 1979) are compared with Wyloo Gp in Ashburton Basin. Geol.prov:Glengarry Sub-basin||||||07-FEB-11
24288|Glengarry Group|65404|6|Mentioned|p245 Fig.1|||||||||
24288|Glengarry Group|65408|6|Mentioned|p81 |Paleoproterozoic|Paleoproterozoic|Originally regarded as western part of Nabberu Basin (Hall and Goode 1978); raised to separate basin status by Gee and Grey (1993). Now redundant: split into three basins and Groups; Yerrida, Bryah and Padbury.||||||
24288|Glengarry Group|65411|5|Briefly described|p88, p90.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979) and Gee and Grey (1993); name abandoned (Pirajno et al. 1996): rocks divided into Bryah and Yerrida Groups.|||Includes Juderina Formation.|||
24288|Glengarry Group|65419|5|Briefly described|pp1-2, p19.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979). In Glengarry Basin as defined by Gee and Grey (1993); formerly part of the Nabberu Basin. Name now obsolete (Pirajno et al. 1996); subdivided into two Groups (Bryah and Yerrida Groups) with different stratigraphic and structural histories, deposited in separate basins; hence Glengarry Basin is discontinued and replaced by Bryah, Yerrida and Padbury Basins.||||||
24288|Glengarry Group|65450|6|Mentioned|p3|||Replaced (in part) by Padbury Group.||||||05-JAN-17
24288|Glengarry Group|65913|6|Mentioned|p3.|||Obsolete term. Its constituents are now assigned to the Bryah, Padbury and Yerrida Groups, each deposited in its separate, eponymous basin.||||||
24288|Glengarry Group|66299|6|Mentioned|p121.|||Daniels (1975); now the Bryah and Yerrida Groups.||||||
24288|Glengarry Group|67346|6|Mentioned|p794|||Of Muhling et al (1978). Replaced by Padbury Group.||||||11-MAY-12
24288|Glengarry Group|67855|5|Briefly described|p198, 204-206, p200, 202, 203, 207, 208|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. Age: < 2.46 Ga adjacent Yilgarn granites and > 1.65 Ga  Earaheedy Group.  |~2.0-1.8 Ga.||Includes Maraloou Formation, Labouchere Formation, Horseshoe Formation, Thaduna Formation, Narracoota Volcanics, Doolgunna Arkose, Johnson Cairn Shale, Juderina Formation, (Finlayson Sandstone).|Overlain by Padbury Group unconfromably.||
24288|Glengarry Group|70804|5|Briefly described|p1-p2|||Divided into the Bryah and Yerrida Groups. Some units previously assigned to this group have been reassigned to the Padbury Group. Also includes the Juderina Formation, Johnson Cairn Shale, Doolgunna Formation, Karalundi Formation, Narracoota Volcanics, Thaduna Greywacke and the Horseshoe Formation.|||Included the Finlayson Sandstone, Maraloou Formation, Crispin Conglomerate.|||27-FEB-23
24288|Glengarry Group|71484|6|Mentioned|p122|||Status: obsolete. Nomenclature proposed by Hall and Goode 1978 to describe stratigraphy in the western part of the Nabberu Basin, and subsequently revised to be part of Bryah Group.||||||30-AUG-19
38126|Glengarry Group""|23525|5|Briefly described|p8|||Superseded - see Glengarry Group.||||||
38126|Glengarry Group""|23781|6|Mentioned|p61|||Superseded by Yerrida and Bryah Groups.||||||
38126|Glengarry Group""|24544|5|Briefly described|p38|||Now the Yerrida and Bryah Groups.||||||
38083|Glenn Herring Shale|23570|4|Described|p233 Appendix 1|||Name should probably be abandoned due to lack of definition and use.  Max. thickness: 24m.||||||
28580|Gnangara sand beds|29767|6|Mentioned|p17|||||||||
36903|Gnewing granodiorite|23383|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Gnewing Granodiorite.  Age: c.1860Ma.||||||07-NOV-08
29782|Gnowangerup Dyke Swarm|43038|6|Mentioned|p9|||||||||
29782|Gnowangerup Dyke Swarm|43498|6|Mentioned|6|||||||||
75966|Gnowangerup dyke swarm|24165|5|Briefly described|Plate 1|Mesoproterozoic|Mesoproterozoic||||||Dolerite dyke (interpreted from aeromagnetic data).|
75966|Gnowangerup dyke swarm|64161|6|Mentioned|p580|Ectasian|Ectasian|1220-1200 Ma. Dolerite. Intrudes Stirling Range Formation||||||
75966|Gnowangerup dyke swarm|70085|6|Mentioned|p234 Fig.1|||Yilgarn Craton.||||||
78592|Gnowangerup-Fraser Dyke Suite|65487|3|Fully described|p5-8, p15, p24, p52, p56-57; Figs. 3,27|Mesoproterozoic|Mesoproterozoic|One of four mafic dyke suites cutting the southern and southeastern Yilgarn Craton. Part of the c.1210 Ma Marnda Moorn Large Igneous Province. Variably E-NE to NE trending; moderately- strongly magnetic. Typically dolerite and gabbro, minor quartz diorite locally. Various ages listed, from 1203 to 1238 Ma.||||||16-JAN-14
78592|Gnowangerup-Fraser Dyke Suite|67268|6|Mentioned|p5, p20||||c. 1210 Ma|||||
78592|Gnowangerup-Fraser Dyke Suite|67722|6|Mentioned|p20|Mesoproterozoic|Mesoproterozoic||c. 1210 Ma(SHRIMP)|||||
78592|Gnowangerup-Fraser Dyke Suite|68186|4|Described|p8, p10, p30, p40-41, p44, p47, p62|Mesoproterozoic|Mesoproterozoic|See also p68-69, Plates 1A, 2. Northern Foreland, Yilgarn Craton. Forms part of the Marnda Moorn Large Igneous Province. Appears as Gnowangerup-Fraser dykes on p8. Moderately to strongly magnetic mafic dykes trending NNE-ENE; mostly interpreted from aeromagnetic data. Several age determinations given in the range 1250-1200 Ma.|c.1210 Ma.|||Intrudes Munglinup Gneiss.|Typically dolerite or gabbro. Unfoliated to schistose, and metamorphosed at greenschist facies.|
78592|Gnowangerup-Fraser Dyke Suite|69003|5|Briefly described|p4, p44-45|||Albany-Fraser Orogen. Part of the Marnda Moorn LIP.|c.1210-c.1170 Ma.||||Voluminous mafic dykes.|
78592|Gnowangerup-Fraser Dyke Suite|69412|5|Briefly described|p1-4, 6, 10-12|||Spaggiari etal. (2009). Yilgarn Craton. Part of the Marnda Moorn Large Igneous Province. Are usually presented in the article as the Gnowangerup-Fraser dykes; sometimes as Gnowangerup dykes and Fraser dykes. Paleomagnetic directions tabulated, discussed in great detail. Dykes strike ENE to NE along the southern and southeasten margins of the Craton.|1210 Ma.||||Medium- to coarse-grained quartz dolerite or gabbro, with intergranular to sub-ophitic textures.|
78592|Gnowangerup-Fraser Dyke Suite|69743|6|Mentioned|p193|||Doyle et al. (2007).|c.1210 Ma.|||Cuts the Tropicana Gneiss.||
78592|Gnowangerup-Fraser Dyke Suite|70084|6|Mentioned|p220|||Albany Fraser Orogen. Associated with Albany-Fraser orogeny (Stage 2). Correlable with the emplacement of the Esperance Supersuite.|ca. 1200 Ma|||||
78592|Gnowangerup-Fraser Dyke Suite|70089|6|Mentioned|p264|||Yilgarn Craton.||||||
78592|Gnowangerup-Fraser Dyke Suite|70182|6|Mentioned|p3|||Yilgarn Craton / Albany-Fraser Orogen.||||||
78592|Gnowangerup-Fraser Dyke Suite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province. Dykes; trending east-northeast to northeast; mostly interpreted from aeromagnetic data.|1218+/-10 Ma- 1202 Ma|Marnda Moorn Supersuite.|||Dolerite and gabbro.|
78592|Gnowangerup-Fraser Dyke Suite|70802|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Albany-Fraser Orogen. Of Marnda Moorn Large Igneous Province. Events: Marnda Moorn Supersuite Magmatic Event (1218-1202 Ma). See 2_5m_interpdykel15_lut.csv, 250k_pre_mesozoic_interpgeol_lut.csv.|1218+\-10 Ma; 1202+\-10 Ma|Unit of Marnda Moorn Supersuite.|||Dolerite and gabbro dykes; trending east-northeast to northeast; mostly interpreted from aeromagnetic data|
78592|Gnowangerup-Fraser Dyke Suite|70826|6|Mentioned|p14 tbl 5|Ectasian|Ectasian|South Yilgarn Craton.|1218-1202 Ma|||||
78592|Gnowangerup-Fraser Dyke Suite|71270|4|Described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Yilgarn Craton, West Australian Craton. Events: Marnda Moorn Supersuite Magmatic Event (1218 - 1202 Ma).|1218+\-10 Ma; 1202+\-10 Ma|Unit of Marnda Moorn Supersuite.|||Dolerite and gabbro dykes; trending east-northeast to northeast; mostly interpreted from aeromagnetic data|
78592|Gnowangerup-Fraser Dyke Suite|71288|6|Mentioned|p136|||Paleomagnetic data from this unit locates Australia in polar latitudes at c.1.2 Ga.||||||
78592|Gnowangerup-Fraser Dyke Suite|71493|5|Briefly described|p42-43|Ectasian|Ectasian|Yilgarn Craton, Eastern Goldfields Superterrane. Age from Wingate et al., (2000). Part of the Marnda Moorn LIP.|1212+/-10 Ma|||||
31929|Gogo formation|43876|14|Not recorded|p561||Frasnian|||||||
31929|Gogo formation|61139|5|Briefly described|p41, p42 Fig. 4|Frasnian|Givetian|Geological Province: Canning Basin.||||||09-JUN-05
23622|Golconda Formation|22774|5|Briefly described|p571|||||||||
23622|Golconda Formation|23146|5|Briefly described|p149|||of Luke Creek Group.||||||
23622|Golconda Formation|23148|5|Briefly described|p112 Table.2|||||||||
23622|Golconda Formation|24160|5|Briefly described|p112.|||||Unit in Luke Creek Group.|||BIF and interlayered mafic rocks.|
23622|Golconda Formation|41885|6|Mentioned|p144|||||||||
23622|Golconda Formation|42533|3|Fully described|p21|||||||||
23622|Golconda Formation|44149|5|Briefly described|p35 fig 2-30, p36, p42 Fig.2-43|Archean|Archean|See also p43 Fig.2-44, p45 Fig.2-48, p57 Fig.2-71. Of Murchison Province||Luke Creek Group||Overlies Murrouli Basalt.|BIF (consisting of quartz, chert, hematite and magnetite in units <10m thick) and interlayered mafic volcanic rocks.|30-JAN-17
23622|Golconda Formation|65268|6|Mentioned|p6 fig 4|||||Luke Creek Group|||Mafic rocks interlayered with quartz-hematite BIF.|
23622|Golconda Formation|69267|5|Briefly described|p652, 654|||Murchison Province, Yilgarn Craton.||Luke Creek Group.||Overlies Murrouli Basalt. Is overlain by Gabanintha Formation.|A sequence of BIF units interlayered with mafic and ultramafic extrusive and intrusive rocks.|
40354|Golconda iron-formation|23922|5|Briefly described|p1241|Archean|Archean|Informal.  Geological Province: Yilgarn Craton.||||||07-NOV-08
40354|Golconda iron-formation|67198|5|Briefly described|p22|Mesoarchean|Mesoarchean|U/Pb zircon age by Mueller and McNaughton (2000).|2912 +/-5 Ma |||||11-SEP-17
32224|Golden Cockatoo Formation|23416|5|Briefly described|Map Legend|Archean|Archean|In the Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|23755|4|Described|p36|Archean|Archean|See also page 17 table 1.||||||07-NOV-08
32224|Golden Cockatoo Formation|23783|4|Described|p15|Archean|Archean|||||||07-NOV-08
32224|Golden Cockatoo Formation|23813|5|Briefly described|p91 Tb. 1|Archean|Archean|Age: >3.24Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|23936|5|Briefly described|Tb.1|Archean|Archean|Age: >3.24 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Cherty, silicate-facies iron formation, rhyolite, quartzite and interbedded peilte.  Max. thickness: 2000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Pilbara Supergroup.  Geological Province: Pilbara Craton||||||07-NOV-08
32224|Golden Cockatoo Formation|24184|4|Described|p702, p696, p699 Fig.3|Archean|Archean|Part of the Yule Granitoid Complex. Geological Province: Pilbara Craton. Age:<3312Ma||||||07-NOV-08
32224|Golden Cockatoo Formation|24531|5|Briefly described|p18|Archean|Archean|Geological Province: Pilbara Craton.  See aso p5 Table 1.||||||07-NOV-08
32224|Golden Cockatoo Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.||||||07-NOV-08
32224|Golden Cockatoo Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|BIF, rhyolite, quartzite, metapelite. Age: >3238Ma. Occurs in the Abydos Belt. Geological Province: Pilbara Craton.||||||07-FEB-11
32224|Golden Cockatoo Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Cherty silicate-facies iron formation, rhyolite, quartzite and interbedded metapelite.||||||07-FEB-11
32224|Golden Cockatoo Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Pilbara Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|50427|5|Briefly described|p182 Fig.5|Archean|Archean|Conformably overlies Kelly Subgroup and Budjan Creek Formation. Overlain by Sulphur Springs Group (generally conformable). Of Pilbara Supergroup.||||||07-NOV-08
32224|Golden Cockatoo Formation|50430|4|Described|p158 Tb.1||Archean|Local in extent. Deposited 3280-3240 Ma. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
32224|Golden Cockatoo Formation|60112|6|Mentioned|p107 Fig.1. |||||||||
32224|Golden Cockatoo Formation|61253|5|Briefly described|p51|Archean|Archean|Comprises metamorphosed clastic sedimentary rocks and banded-iron formation.  Age: 3192+/-74Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|61266|4|Described|p58 Tb.1, p59|Archean|Archean|Age: >3238 Ma. Cherty silicate-facies iron formation, rhyolite, quartzite and interbedded metapelite. Geological Province: Pilbara Craton.||||||07-NOV-08
32224|Golden Cockatoo Formation|63441|4|Described|p21|Archean|Archean|Of Van Kranendonk and Morant (1998). Name abandoned - components reassigned into: ultramafics into Kunagunarinna Fm., mafic + felsic volcanic rocks, metased.rocks and BIF into Kangaroo Caves Fm. Folded rocks unconform.on Callina/Tambina Sup'suite granites||||||07-FEB-11
32224|Golden Cockatoo Formation|64328|5|Briefly described|p56 Tb. 1|||Sandstone, shale.||||||07-FEB-11
32224|Golden Cockatoo Formation|65825|6|Mentioned|p5. |Archean|Archean|||Unit in Pilbara Supergroup according to Van Kranendonk et al. (2001, 2002).||||
32224|Golden Cockatoo Formation|69167|6|Mentioned|160956.1.pdf|||Discontinued group. Age derived from sample of coarse grained feldspathic sandstone (178045) and is the maximum age of sandstone deposition.|3192 +/- 74 Ma (SHRIMP)|||||
32224|Golden Cockatoo Formation|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. No longer current.||||||
32224|Golden Cockatoo Formation|69590|5|Briefly described|160956.1.pdf + other geochron files|||Formerly mapped to include the Kangaroo Caves Formation (Van Kranendonk and Morant, 1998; Van Kranendonk, 2000), and interpreted to occupy a stratigraphic position betwenn Euro Basalt and Sulphur Springs Group. Sample GSWA 178045 (sandstone) yielded an interpreted maximum depositional age of 3192+\-74 Ma for the sandstone (weighted mean 207Pb/206Pb).||||||
40545|Golden Grove Formation|23955|4|Described|p1239, p1242 Fig.3|Archean|Archean|Overlain by the Scuddles Formation. Overlies the Gossan Valley Formation. Maximum Thickness: 550m. Geological Province: Yilgarn Craton. Divided into 6 members.||||||10-MAY-11
40545|Golden Grove Formation|61912|5|Briefly described|p158|||Layered rhyodacitic volcaniclastic succession subdivided into 6 members.||||||
40545|Golden Grove Formation|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain. See also Golden Grove Group (p51, p53).||Minjar Group.||||
40545|Golden Grove Formation|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Minjar Group||Overlies the Gossan Valley Formation, overlain by the Scuddles Formation.|Felsic volcaniclastic and volcanic rocks.|
40545|Golden Grove Formation|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Minjar Group.||||
40545|Golden Grove Formation|70020|4|Described|p128,131|||Geological province: Yilgarn Craton. Thickness between 75-800m. Characterised by products of distal explosive felsic volcanism, re-deposited by successive mass flow processes.  Hosts numerous base metal deposits.||Unit of Gossan Hill Group.||Overlain by Scuddles Formation. Underlain by Gossan Valley Formation.|Rhyolite to andesite tuffaceous volcaniclastic sediments, minor sedimentary anf felsic volcanic rocks including andesite, rhyodacite and dacite.|16-JUL-19
40545|Golden Grove Formation|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Mount Gibson Group.||Upper unit of Mount Gibson Group. Overlain (?disconformably) by Murrouli Basalt. Underlain by Orion Formation.||
40545|Golden Grove Formation|70270|4|Described|p519-523, p525-533, p535-537, p538|||Murchison Province. 75-800m thick. Includes extensive descriptions of massive sulfide deposits. Subdivided into 6 informal members based on facies grain-size variation, the abundance of volcanic quartz grains, and bedding characteristics. Lithological descriptions of members given. Said to be deposited in a sub-aqueous environment.||Of Gossan Hill Group||Overlain by Scuddles Formation. Overlies Gossan Valley Formation.|Bedded tuffaceous volcaniclastic rocks. Quartz rich sandstone, pebble breccia; tuffaceous clasts. Granule breccia. Sst laminated to massive. Lenses of polymict pebble breccia include pyrite clasts. Thin chert beds interbedded w sandstone-siltstone.|29-JUN-18
40545|Golden Grove Formation|71168|4|Described|p11, p12 fig 6|||Yilgarn Craton. Hosts the Gossan Hill copper and zinc deposits. Appears as the Golden Grove formation on p11. Thickness ranges from 75 to 800m thick. See also p13 fig 7, p50 fig 29, p57-p58.||Gossan Hill Group||Overlies the Gossan Valley Formation. Overlain by the Scuddles Formation.|Rhyolite to andesite tuffaceous volcaniclastic sediments; minor sedimentary and felsic volcanic rocks including andesite, rhyodacite and dacite.|
40545|Golden Grove Formation|73596|6|Mentioned|p1170|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton.|c.2960-2945 Ma.|Golden Grove Group.||||
36116|Golden Grove Group|23441|5|Briefly described|p163|Archean|Archean|2957-2951Ma||||||07-NOV-08
36116|Golden Grove Group|66195|6|Mentioned|p611 Fig.9|Mesoarchean|Mesoarchean|Of Murchison Supergroup. Underlies the Norie Group||||||
36116|Golden Grove Group|67129|5|Briefly described|p17-18, p20, p55|Archean|Archean|Southern Murchison Domain, Youanmi Terrane. Accompanied by widespread intrusion of synvolcanic granite plutons with common c.2950 Ma xenocrystic zircons indicating authochthonous development on older crust.|2960-2930 Ma|Murchison Supergroup|||Felsic and mafic volcanics and volcaniclastic rocks.|07-SEP-17
36116|Golden Grove Group|68108|5|Briefly described|p628, p650, p651 Tb.4|Mesoarchean|Mesoarchean|NE Murchison Domain, Youanmi Terrane. Geochronology by Wang et al. (1998).|ca. 2960-2930 Ma||||Felsic volcanics.|
36116|Golden Grove Group|68109|5|Briefly described|p659|Mesoarchean||Murchison Domain.|> 2900 Ma|Of the Murchison Supergroup.||||
36116|Golden Grove Group|68698|5|Briefly described|p2, p4, p19|Mesoarchean|Mesoarchean|Murchison Domain, Yilgarn Craton.||Murchison Supergroup.|Mount Gibson Formation.|||
36116|Golden Grove Group|69583|6|Mentioned|p51, p53|Mesoarchean|Mesoarchean|See also Golden Grove Formation (p49).||||||
36116|Golden Grove Group|71168|6|Mentioned|p10|Mesoarchean|Mesoarchean|Burtville Terrane, Yilgarn Craton.|>2900 Ma|||||
36116|Golden Grove Group|73596|6|Mentioned|p1170|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton.||Murchison Supergroup.|Golden Grove, Honman Formations; Southern Cross Microgranite.|Is overlain by Norie Group.||
34797|Golden Grove Unit|22774|5|Briefly described|p572, Fig.2 p573|||See also Fig.3 p574||||||
32585|Golden Mile Basalt|45546|14|Not recorded|p.51|||Should be Golden Mile Dolerite.||||||
41083|Golden Mile dolerite|24139|5|Briefly described|p239 Table 1|||Geological Province: Kambalda Domain. Of the Black Flag Beds.||||||
41083|Golden Mile dolerite|60978|6|Mentioned|p68-69 Fig.3|||Informal reference to a dolerite in the Kalgoorlie region. Geological Province: Yilgarn Craton.||||||
41083|Golden Mile dolerite|62083|5|Briefly described|p1010, p1014, p1015 Fig.7|||Significant host for gold.||||Emplaced near contact between Kambalda Group and Black Flag Group.|Dolerite sill; granophyric. Fractionated mafic layered sills.|
83342|Golden Valley conglomerate|68154|5|Briefly described|p110|||Contains meta-sandstone of volcaniclastic origin with an MDA of 2668 +/- 7 Ma.|<2668 Ma.||||A sequence of E-dipping, structurally dismembered sandstones and conglomerates.|
80207|Golden Valley member|71166|5|Briefly described|p23|||[An informal, probable company name from the Kanowna gold camp]|||||Conglomerate, sandstone, volcaniclastic sedimentary rocks.|
80207|Golden Valley member|73391|4|Described|p132, 148, 159-166, 174, 182-183, 189|||See also p194, 196, 224, 244, 247, 444. Kanowna district. Three sub-units are Golden Valley felsic unit, Golden Valley conglomerate, and the topmost Golden Valley sandstone. Lithologies described in detail: stratigraphic column, clast/matrix diagrams, photographs, photomicrographs. See references to Golden Valley Conglomerate (p26, 51, 161-163, 165-166, 189-191, 199, 224, 241, 304, 413, Appendix p110).|2668 +/- 9 Ma (MDA: Ross et al., 2004).|Black Flag Formation.||Unconformably overlies Perkolilli rhyolite. Is overlain by Grave Dam member and (unconformably) Panglo member. Time equivalent or overlies Grave Dam Grit/member.|A lower section of felsic grit with interbedded volcanic breccia and felsic conglomerate; a central section of conglomerates, grits and sandstone; an upper section of sandstone and thin conglomerate interbeds.|
83948|Golden Valley turbidite|70482|5|Briefly described|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.||Kalgoorlie Sequence.||Conformably overlies Golden Valley Conglomerate.|Feldspar-rich volcanic sandstone, siltstone and lesser mudstone.|
83490|Goldern Grove Group|73453|5|Briefly described|p3|Mesoarchean|Mesoarchean|Youanmi Terrane (Murchison).|2960-2935 Ma||||Felsic volcanics.|
69690|Goldsworthy Group|61253|5|Briefly described|p53, p52 Fig. 2|Archean|Archean|Eroded and deformed remnants of the De Grey Supergroup; consists dominantly of coarse-grained clastic sedimentary rocks. Geological Province: Lalla Rookh / Pilbara Craton.||||||07-NOV-08
73950|Goldwyer Formation Carbonates|61021|6|Mentioned|p38|||Informal - refers to hydrocarbon reservoir rocks of the Goldwyer Formation.||||||17-DEC-07
73951|Goldwyer Formation Shales|61021|6|Mentioned|p38|||Informal - refers to hydrocarbon seal rocks of the Goldwyer Formation.||||||17-DEC-07
77742|Goldwyer Formation, Lower|64975|5|Briefly described|pp163-165.|Ordovician|Ordovician|Informal term for the stratigraphically lower (200 m deeper) hydrocarbon source interval in the Goldwyer Formation. Contains lower proportion of G. prisca and more amorphous organic material and acritarchs.||||||
77743|Goldwyer Formation, Upper|64975|5|Briefly described|pp163-164.|Ordovician|Ordovician|Informal term for the stratigraphically higher hydrocarbon source interval in the Goldwyer Formation. The cyanobacteria Gloeocapsomorpha prisca comprises bulk of preserved organic material. Saturate fraction has a composition unique in WA.||||||
39713|Goldwyer formation, upper|24449|6|Mentioned|p746|||Informal - see Goldwyer Formation.||||||
34879|Googenhama Formation|22907|6|Mentioned|41|||Misspelling of Googhenama Formation.||||||
34879|Googenhama Formation|71042|6|Mentioned|p72|||Mis-spelling of the Googhenama Formation.||||Unconformably overlies the Manganese Group, Carawine Dolomite and Pinjian Chert Breccia. Overlies the Jeerinah and Maddina Formations.||
70752|Googhenama Conglomerate''|62453|6|Mentioned|p63|||Informal Name.||||||
37934|Goongarrie-Mount Pleasant granite|24305|6|Mentioned|p926|||Not intended as a formal stratigraphic name.||||||
40745|Gooragoora Member|24183|6|Mentioned|p10|||Informal name - redefined and elevated to Gooragoora Formation.||||||
37993|Gooragoora Sandstone|22905|6|Mentioned|p52 Fig. 2|Mesoproterozoic|Mesoproterozoic|See also Gooragoora Sandstone Member.  Now upgraded to Gooragoora Formation.||||||24-JAN-06
37993|Gooragoora Sandstone|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of Irregully Formation.||||||
37993|Gooragoora Sandstone|24183|5|Briefly described|p4 Fig.3|Mesoproterozoic|Mesoproterozoic|Of the Florry Subgroup (Chuck 1984)||||||
37993|Gooragoora Sandstone|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Florry Subgroup. Superseded by Gooragoora Formation. Overlies Irregully Formation. Overlain by Blue Billy Formation.||||||
37993|Gooragoora Sandstone|44142|4|Described|p314 Tb.4-4, p317-318, p326 Tb.4-5|||10-250m thick lenticular (discontinuous) units of alluvial fan, fan delta and marine deposits. Originally Gooragoora Sandstone Member of Irregully Formation; a correlate of Prairie Downs Member (now named Prairie Downs Formation). Within Florry Subgroup of Chuck (1984). Appears as Goorogoora Sandstone in Tb.4-5.||Edmund Subgroup.||Overlies Irregully Formation (conformably). Overlain by Cheyne Springs Formation.|Medium-grained sandstone, some shale, conglomerate.|13-MAR-18
37993|Gooragoora Sandstone|50225|5|Briefly described|p387 Fig. 2|||Of the Edmund Subgroup (Bangemall Group). Now superseded by Gooragoora Formation.||||||07-FEB-11
38597|Gorge Creek Group""|23783|6|Mentioned|p23|Archean|Archean|Informal name - see Gorge Creek Group.||||||07-NOV-08
74150|Gorge Creek Supergroup|62979|6|Mentioned|p215, p218|||Geological Province: Pilbara Craton.||||||07-FEB-11
23633|Gossan Hill Group|23955|4|Described|p1240, p1242 Fig.3|||Overlain by the Thundelarra Group. Maximum Thickness: 3100m. Geological Province: Murchison province, Yilgarn Craton.||||||
23633|Gossan Hill Group|41066|5|Briefly described|1 of 2 J05|||||||||
23633|Gossan Hill Group|41434|5|Briefly described|p920|||||||||
23633|Gossan Hill Group|43768|6|Mentioned|p874|||||||||
23633|Gossan Hill Group|69584|6|Mentioned|p59|Mesoarchean|Mesoarchean|[Obsolete name, replaced with the Gossan Hill Formation]. Golden Grove.|2960-2945 Ma (SHRIMP U-Pb, Wang et al, 1998)|||||
23633|Gossan Hill Group|70020|4|Described|p131|||Geological province: Yilgarn Craton. Thickness: 2800-3100m.||Unit of Murchison Supergroup.|Includes Cattle Well Formation, Scuddles Formation, Golden Grove Formation, Gossan Valley Formation and Shadow Well Formation.|Overlain by Thundelarra Group. Underlain unconformably by Murchison Monzogranite.||
23633|Gossan Hill Group|70270|5|Briefly described|p519 Fig. 2, p520 Fig. 3|||After Clifford, 1992 PhD. Murchison Province.||Of Murchison Supergroup.||||
23633|Gossan Hill Group|71168|5|Briefly described|p11, p12 fig 6, p13 fig 7|||Yilgarn Craton. |||Includes the Shadow Well Formation, Gossan Valley Formation, Golden Grove Formation, Scuddles Formation and the Cattle Well Formation.|||
40546|Gossan Valley Formation|23955|4|Described|p1241 Fig.2, p1242 Fig.3|||Overlain by the Golden Grove Formation. Overlies the Shadow Well Formation. Maximum Thickness: 920m. Geological Province: Murchison province, Yilgarn Craton.||||||
40546|Gossan Valley Formation|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Minjar Group.||||
40546|Gossan Valley Formation|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Minjar Group||Overlain by the Golden Grove Formation, overlies the Madoonga Formation.|Komatiitic basalt, felsic volcaniclastic and volcanic rocks.|
40546|Gossan Valley Formation|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Minjar Group.||||
40546|Gossan Valley Formation|70020|4|Described|p131|||Geological province: Yilgarn Craton. Thickness: 170-920m.||Unit of Gossan Hill Group.||Overlain by Golden Grove Formation. Underlain by Shadow Well Formation.|Polymict sandstone and breccia, minor dacite, rhyolite and mafic volcanic rocks.|
40546|Gossan Valley Formation|70270|5|Briefly described|p519 Fig. 2, p520 Fig. 3, p521|||Probably after Clifford, 1992 PhD. Murchison Province. 170-920m thick.||Of Gossan Hill Group||Shown as underlying Golden Grove Formation. Shown as overlying the Shadow Well Formation.|Polymict sandstone and breccia, minor dacite, rhyolite and mafic volcanic rocks|29-JUN-18
40546|Gossan Valley Formation|71168|4|Described|p11, p12 fig 6, p13 fig 7, p57|||Yilgarn Craton. Appears as the Gossan Valley formation on p11. Thickness ranges from 170 to 920m.||Gossan Hill Group||Overlies the Shadow Well Formation. Overlain by the Golden Grove Formation.|Polymict sandstone and breccia, minor dacite, rhyolite, and mafic volcanic rocks.|
34798|Gossan Valley Unit|22774|5|Briefly described|p572, Fig.2 p573|||See also Fig.3 p574||||||
77710|Gosselin group|60372|5|Briefly described|pp86-103.|||Informal name for a later component of Bunbury Basalt. Continental flood basalt eruption at c.123 Ma. More contaminated by continental lithosphere than Casuarina group basalts.|123 Ma (Coffin et al, 2002)|||||06-FEB-18
80939|Government Dam Grit|72049|6|Mentioned|p259, 269|||Near Kanowna Belle.||Of Early Merougil Group.||||18-MAR-19
83949|Government Dam turbidite|70482|6|Mentioned|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Over 300m thick. Contact with Grave Dam Grit not exposed.||Kalgoorlie Sequence.|||Quartz-rich sandstone, siltstone and lesser mudstone; turbidites; beds up to several tens of cms thick.|
78799|Granites Tanami Complex|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||||||
77548|Granny Smith Sequence|66880|6|Mentioned|p28.|Archean|Archean|As distinct from the formally-named unit, the Granny Smith Granodiorite. This unit is said to be a siliciclastic sequence, an upwards continuation of the Wallaby Sequence.|2663 +/- 5 Ma.|||||
35826|Granny Smith diorite|23320|6|Mentioned|p423|||Informal name. Mafic granitoid rocks.||||||07-FEB-07
72766|Granny Smith granodiorite|62106|5|Briefly described|p1375, p1376, p1377|Archean|Archean|Informal reference to granodiorite rock in the Granny Smith gold deposit. Age: 2665+/-4 Ma. Geological Province: Laverton greenstone belt in Eastern Goldfields province of Yilgarn Craton.||||||07-NOV-08
72766|Granny Smith granodiorite|67198|6|Mentioned|p52 |||||||||
72766|Granny Smith granodiorite|70271|5|Briefly described|p541, 554|||Laverton area, Eastern Goldfields province, Yilgarn Craton. Hosts the Granny Smith gold deposit, which is dated 30 m.y. after crystallisation of the granodiorite. See also reference to Granny Smith Granodiorite (p556).|2665 +/- 4 Ma; U-Pb SHRIMP (Ojala et al., 1997).|||||
77562|Granny Supersequence|66937|5|Briefly described|p155, pp168-170.|Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin. At least 1465 m thick.||||time equivalent to Santa Claus Member of Belches Supersequence|Dominantly mudrock with pebble conglomerate and sandstone, divided into lower and upper successions by 200 m of sandstone, mudrock and banded iron formation.|02-NOV-12
77562|Granny Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
25934|Grant Formation|22764|4|Described| Table 2, p10|Early Permian|Late Carboniferous|1000 m. Disconformable beneath Poole Sandstone.||||||01-FEB-10
25934|Grant Formation|23757|5|Briefly described|p5|Early Permian|Early Permian|Of Leech (1979b).  Superseded by  Grant Group, but see also "Grant Formation" . Geological Province: Canning Basin.||||||07-JAN-08
25934|Grant Formation|24061|4|Described|p181|Early Permian|Late Carboniferous|Geological Province:  Canning Basin.||||||
25934|Grant Formation|24062|5|Briefly described|p186 Table 1|Permian|Permian|Geological Province: Canning Basin.||||||
25934|Grant Formation|24246|6|Mentioned|p15|Permian|Carboniferous|Geological Province: Canning Basin||||||24-FEB-05
25934|Grant Formation|29591|6|Mentioned|p105|||||||||
25934|Grant Formation|29813|6|Mentioned|p16|||||||||
25934|Grant Formation|29817|5|Briefly described|p8|||||||||
25934|Grant Formation|29818|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous to Lower Permian.||||||
25934|Grant Formation|29819|6|Mentioned|Map legend|Early Permian|Early Carboniferous|Upper Carboniferous to Lower Permian?||||||
25934|Grant Formation|30110|6|Mentioned|p81|||See also P83. Sakmarian age.||||||
25934|Grant Formation|30313|4|Described|p54|||Lower Permian age.||||||
25934|Grant Formation|30338|4|Described|p100|||||||||
25934|Grant Formation|30340|5|Briefly described|p2533|||||||||
25934|Grant Formation|30341|5|Briefly described|p145|||||||||
25934|Grant Formation|30342|6|Mentioned|p103|||||||||
25934|Grant Formation|30525|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
25934|Grant Formation|30533|4|Described|p25|||On Table 7.||||||
25934|Grant Formation|30545|6|Mentioned|Fig.2|||Sakmarian||||||
25934|Grant Formation|30595|5|Briefly described|p3|||||||||
25934|Grant Formation|30897|4|Described|p18|||||||||
25934|Grant Formation|30898|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
25934|Grant Formation|31047|6|Mentioned|Fig. 2|||Stratigraphic section through Canning Basin.||||||
25934|Grant Formation|31251|6|Mentioned|p68|||Refers Crespin (1958)||||||
25934|Grant Formation|31332|6|Mentioned|Fig. 3|||||||||
25934|Grant Formation|31706|6|Mentioned|p657|||Permian correlation chart||||||
25934|Grant Formation|31870|6|Mentioned|p128|||||||||
25934|Grant Formation|32094|6|Mentioned|p382|||||||||
25934|Grant Formation|32376|6|Mentioned|p1541|||||||||
25934|Grant Formation|32648|6|Mentioned|p32|||L. Perm.||||||
25934|Grant Formation|32865|6|Mentioned|p476|||Lower Permian. See also P477||||||
25934|Grant Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
25934|Grant Formation|33042|6|Mentioned|Fig.1|||Permian. See also Fig.4||||||
25934|Grant Formation|33518|4|Described|Table 1|||||||||
25934|Grant Formation|33519|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
25934|Grant Formation|33622|6|Mentioned|p89|||||||||
25934|Grant Formation|33701|6|Mentioned|Fig.1|||Sakmarian||||||
25934|Grant Formation|33960|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous to Lower Permian||||||
25934|Grant Formation|33962|6|Mentioned|p50|||||||||
25934|Grant Formation|33965|4|Described|Table 1|||Mention p6.||||||13-NOV-07
25934|Grant Formation|33966|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous - Lower Permian||||||
25934|Grant Formation|34085|6|Mentioned|Cor.chart|||Stephanian||||||
25934|Grant Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
25934|Grant Formation|34287|6|Mentioned|p125|||||||||
25934|Grant Formation|34532|6|Mentioned|p219|||Sakmarian.  See P225||||||
25934|Grant Formation|35104|6|Mentioned|p4|||||||||
25934|Grant Formation|35119|6|Mentioned|p462|Permian|Carboniferous|Overlies Nita Formation in Dampier Downs 1.||||||21-APR-17
25934|Grant Formation|35120|6|Mentioned|Map legend|Early Permian|Late Carboniferous|||||||
25934|Grant Formation|35124|6|Mentioned|Map legend|Early Permian|Late Carboniferous|||||||
25934|Grant Formation|35205|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25934|Grant Formation|35225|6|Mentioned|p5|||||||||
25934|Grant Formation|35226|6|Mentioned|p5|||||||||
25934|Grant Formation|35275|6|Mentioned|Fig.5.|||||||||
25934|Grant Formation|35711|4|Described|p24|||See also Table 3, stratigraphy||||||
25934|Grant Formation|35914|5|Briefly described|p6|||||||||
25934|Grant Formation|35969|6|Mentioned|Fig.10|||See also Table 7.||||||
25934|Grant Formation|35983|6|Mentioned|Table 28|||||||||
25934|Grant Formation|36020|6|Mentioned|p388|||||||||
25934|Grant Formation|36253|6|Mentioned|p131|||||||||
25934|Grant Formation|36365|6|Mentioned|p816|||||||||
25934|Grant Formation|36596|6|Mentioned|Text Fig.2|||||||||
25934|Grant Formation|36718|6|Mentioned|p460|||||||||
25934|Grant Formation|36890|3|Fully described|p339|||See also p344.||||||13-NOV-07
25934|Grant Formation|37065|6|Mentioned|p30|||||||||
25934|Grant Formation|37106|5|Briefly described|p277|||||||||
25934|Grant Formation|37295|6|Mentioned|p52|||||||||
25934|Grant Formation|37914|6|Mentioned|p449|||||||||
25934|Grant Formation|37926|6|Mentioned|p499|||||||||
25934|Grant Formation|38217|6|Mentioned|p269|||||||||
25934|Grant Formation|38263|6|Mentioned|p12|||||||||
25934|Grant Formation|38301|6|Mentioned|p279|||||||||
25934|Grant Formation|39307|6|Mentioned|p44|||||||||
25934|Grant Formation|39757|6|Mentioned|p1606|||||||||
25934|Grant Formation|39796|6|Mentioned|Map legend|Permian|Permian|||||||
25934|Grant Formation|39854|6|Mentioned|p18|||||||||
25934|Grant Formation|40417|6|Mentioned|p67|||||||||
25934|Grant Formation|40636|6|Mentioned|p44|||||||||
25934|Grant Formation|40793|6|Mentioned|p171|||||||||
25934|Grant Formation|40837|6|Mentioned|Fig.14|||||||||
25934|Grant Formation|40838|6|Mentioned|p281|||||||||
25934|Grant Formation|40866|6|Mentioned|p179|||||||||
25934|Grant Formation|41023|6|Mentioned|Fig.5|||||||||
25934|Grant Formation|41125|5|Briefly described|p42|||||||||
25934|Grant Formation|41315|5|Briefly described|p135|||||||||
25934|Grant Formation|41894|6|Mentioned|p2|||||||||
25934|Grant Formation|41913|6|Mentioned|p106|||||||||
25934|Grant Formation|41918|5|Briefly described|p97|||||||||
25934|Grant Formation|42062|6|Mentioned|p26|||||||||
25934|Grant Formation|42392|6|Mentioned|p115|||Misspelling of Grant Group?||||||
25934|Grant Formation|42930|5|Briefly described|Fig.1 p473|Early Permian|Late Carboniferous|Unconformably underlies Poole Sandstone. Geological Province: Canning Basin. Marine and glacial deposits.||||||13-NOV-07
25934|Grant Formation|43173|5|Briefly described|12-54|Early Permian|Late Carboniferous|||||||
25934|Grant Formation|43599|6|Mentioned|p251|||||||||
25934|Grant Formation|43932|4|Described|p4,Tb.1 p6|Early Permian|Late Carboniferous|||||||
25934|Grant Formation|44040|14|Not recorded|p40,42,43|||||||||
25934|Grant Formation|44064|14|Not recorded|p55|||||||||
25934|Grant Formation|44100|14|Not recorded|p42|||||||||
25934|Grant Formation|44219|14|Not recorded|p31||Sakmarian|||||||
25934|Grant Formation|44356|5|Briefly described|p9,Tb.1 p6|Sakmarian|Late Carboniferous|||||||
25934|Grant Formation|44366|14|Not recorded|p.20|||||||||
25934|Grant Formation|44397|14|Not recorded|p.20,22,Fig.3, Tb.4|||L.Perm-U. Carb. See also p.12,13,18.||||||
25934|Grant Formation|44398|14|Not recorded|map legend||Permian|||||||
25934|Grant Formation|44403|2|Defined|p.5,6,7,8,9,11,12|||E/51-12, unconformably overlies Laurel Beds, disconformably underlies Poole Sandstone.||||||13-NOV-07
25934|Grant Formation|44404|14|Not recorded|map legend||Permian|||||||
25934|Grant Formation|44479|2|Defined|Tb.1|||E/51-1. Correlates with Cuncudergerie Sandstone of this Sheet.||||||
25934|Grant Formation|44499|14|Not recorded|opp.p.6, Tb.1||Permian|||||||
25934|Grant Formation|44994|6|Mentioned|Fig.7|||Correlation. L. Perm.||||||
25934|Grant Formation|44998|2|Defined|p70-2|Sakmarian|Stephanian|U.Stephanian-Sakmarian. On many pages. p.19,20,38-9,42,50,58-62,67,76,78-9,83,87,91,99-103,132,220-9,238-9,244-6, App.2 p268,App.3 p278, App.6 p293,306.||||||
25934|Grant Formation|45016|14|Not recorded|p.18,31|||Tb (back). Lower part correlated with Austin Formation.||||||
25934|Grant Formation|45041|6|Mentioned|Fig.45|||L.Perm.||||||
25934|Grant Formation|45063|6|Mentioned|Fig. 9|||Carboniferous||||||
25934|Grant Formation|45097|5|Briefly described|p26|||Refers Balme(in Johnstone,'68). Microflora. ?outcrop identification.||||||
25934|Grant Formation|45101|6|Mentioned|Fig.8|||||||||
25934|Grant Formation|45104|6|Mentioned|p29|||||||||
25934|Grant Formation|45133|6|Mentioned|p2|||||||||
25934|Grant Formation|45140|5|Briefly described|p67|Permian|Late Carboniferous|Canning Basin.||||Unconformably overlies Knobby Sandstone. Is overlain conformably by Poole Sandstone.|Mainly fluvial sandstone.|
25934|Grant Formation|45143|6|Mentioned|p4|||||||||
25934|Grant Formation|45153|2|Defined|App.4-58|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian. Formerly Grant Range beds.||||||
25934|Grant Formation|45923|14|Not recorded|p.71||Permian|||||||
25934|Grant Formation|46849|6|Mentioned|p177|||||||||
25934|Grant Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
25934|Grant Formation|48573|14|Not recorded|p.3,8,13,14,21 pl.1.||| O/lies Anderson Fm.||||||
25934|Grant Formation|48596|14|Not recorded|p.5,19, Pl.1|||(E51-11)||||||
25934|Grant Formation|48826|2|Defined|p.21||Sakmarian|Tb.III, p.1,21,22,37,40,Pl.1. Correlates with Braeside Tillite and Paterson Formation. Overlain by Condren Sandstone Member. (E52-13,14,F52-2).||||||13-NOV-07
25934|Grant Formation|48831|14|Not recorded|p.37|||||||||
25934|Grant Formation|48837|14|Not recorded|p.21|||On many pages. p.1,6,7,11-13,16,18,21-22,24,25,26,27,30.||||||
25934|Grant Formation|48842|14|Not recorded|p.22,Tb.I|||||||||
25934|Grant Formation|48874|14|Not recorded|p.3,12,16|||Negative anomaly.||||||
25934|Grant Formation|48978|6|Mentioned|p4|||U.Carb.-L.Perm.||||||
25934|Grant Formation|48995|6|Mentioned|p12|||[Superseded by Grant Group. CEBMar95]||||||
25934|Grant Formation|61020|6|Mentioned|p33 Fig. 4|||Lead for petroleum potential.  Geological Province: Canning Basin.||||||20-APR-05
25934|Grant Formation|64185|5|Briefly described|p158 Fig. 2, p159, p165|Early Permian|Late Carboniferous|Underlain by Lennard River Group. Overlain by Wallal Sandstone. Marine - marginal marine - fluvoglacial. See p165 for more information.||||||
25934|Grant Formation|64186|4|Described|p171, p170 Fig. 1|Sakmarian|Stephanian|Overlain by Poole Sandstone, underlain by Carribuddy Formation. Max thickness: 500m. Glacigene sequence of tillite, sandstone, siltstone and shale.||||||
25934|Grant Formation|64187|5|Briefly described|p320 Fig. 2, p321|Permian|Carboniferous|Underlain unconformably by Anderson Formation, overlain by Poole Sandstone. Sandstone, shale (fluvio-glacial marine). Geological Province: Canning Basin.||||||03-FEB-10
25934|Grant Formation|66949|6|Mentioned|p9, p13; p74-75,83 Appx.5|||Guppy et al. (1952). Originally Grant Range Beds (Woolnough, 1933). Subsequently Grant Group (Crowe and Turner, 1976).||||||
25934|Grant Formation|70288|6|Mentioned|p415|Pemian|Permian|See also references to Grant Group (p414-415, 417-419).|||||Sandstone.|
25934|Grant Formation|71171|6|Mentioned|p7|||Revised and renamed to the Grant Group.||||||
25934|Grant Formation|73117|6|Mentioned|p2, p117, p120, p126, p130, p132|||(Guppy et al., 1952). [Superseded; see Grant Group]. [Written as 'Grant Formation' and 'Grant formation'].||||||
28585|Grant Formation (Upper)|41730|6|Mentioned|p471|||See also p498. [Superseded by Grant Group. CEBMar95]||||||05-NOV-15
78586|Grant Formation, Lower""|44143|6|Mentioned|p443|Carboniferous|Carboniferous|Of Goldstein and Hubbard (1984). A pre-glacial unit of Westphalian age, considered to overlie the Visean-Namurian Anderson Formation.||||||19-DEC-13
78586|Grant Formation, Lower""|66949|6|Mentioned|p78 Appx.5|||Equivalent to Reeves Formation.|||||Includes sandstone.|
83353|Grant Formation, Lower''|73117|6|Mentioned|p22|||Of Goldstein and Hubbard (1984). [Written as 'Lower Grant Formation' on p22 and 'lower Grant' or 'pre-Grant' formations on p2 probably in reference to strata now called the Reeves Formation].||||||
39291|Grant Group sandstones|24246|6|Mentioned|p14|Permian|Carboniferous|Geological Province: Canning Basin.||||||
39291|Grant Group sandstones|61021|6|Mentioned|p39|Early Permian|Late Carboniferous|Informal- refers to sandstones within the Grant Group.||||||17-DEC-07
83354|Grant Group shale, mid-''|73117|6|Mentioned|p32|||[Written as 'mid-Grant Group shale']. A [informal] term for a mudstone horizon(s) within the Grant Group that is(are) not included in the Calytrix Formation (the latter being largely restricted to the Barbwire Terrace). Appears to represent several disparate horizons extending up to a few tens of kilometres along the Lennard Shelf.||||||
40308|Grant Group shales, Upper|24390|5|Briefly described|p8|||Informal-see Grant Group.  Geological Province: Canning Basin.||||||
40308|Grant Group shales, Upper|50085|5|Briefly described|p8|Permian|Permian|Informal - see Grant Group.  Geological Province: Canning Basin.||||||
83337|Grant Group''|73117|6|Mentioned|26|||[A variation on Grant Group probably written in inverted commas to denote particular usage].||||||
40477|Grant Group, Lower|24466|5|Briefly described|p367|||Now named the Reeves Formation.||||||
40477|Grant Group, Lower|62837|5|Briefly described|Stratigraphic columns|Namurian|Namurian|Informal name.  Age: ~312-320. Geological Province:  Fitzroy Trough.||||||
40477|Grant Group, Lower|64971|6|Mentioned|p683, p684, p685 Fig. 2|Early Permian|Carboniferous|||||||09-FEB-10
40477|Grant Group, Lower|69693|6|Mentioned|p3|Carboniferous|Carboniferous|||||||
40478|Grant Group, Upper|13255|6|Mentioned|p369|Permian|Permian|Roebuck Basin. Early Permian.||||Is overlain by Poole Sandstone.||
40478|Grant Group, Upper|13354|6|Mentioned|p376 Fig.7.|Early Permian|Early Permian|Onshore Canning Basin. Separated from overlying Poole Sandstone by an unconformity of Sakmarian age. Marine shales and limestones. Equivalent to Kuriyippi Formation and Treachery Shale of Bonaparte Basin.||204||||28-OCT-14
40478|Grant Group, Upper|24466|5|Briefly described|p367|||Now known as the Grant Group.||||||
40478|Grant Group, Upper|62837|5|Briefly described|Stratigraphic columns|||Informal name.  Age: ~297->290. Geological Province:  Fitzroy Trough.||||||
40478|Grant Group, Upper|64971|6|Mentioned|p683, p684, p685 Fig. 2|Early Permian|Carboniferous|||||||09-FEB-10
39660|Grant Group, lower|24449|6|Mentioned|p750|||Informal - see Grant Group.  See also p742 Fig. 4A.||||||
39660|Grant Group, lower|72497|6|Mentioned|p3 Fig.2, p4, p13, p17|Moscovian|Serpukhovian|Age shown as Namurian-Westphalian ~= Serpukhovian-Moskovian.||||Unconformably overlies Anderson Formation and underlies Grant Group, upper.||
83338|Grant Group, lower''|73117|6|Mentioned|p19, p111|||[Obsolete? Written as 'lower Grant Group' to indicate specific usage]. Common term in older well completion reports in reference to strata that is now the Reeves Formation.||||||
82136|Grant Group, upper|72497|6|Mentioned|p1, p3 Fig.2, p4, p5, p10, p14, p17.|Sakmarian|Gzhelian|Age shown as Stephanian- Sakmarian ~= Gzhelian-Sakmarian. See also p19.||||Unconformably underlies Poole Sandstone and Nura Nura Member.||
75239|Grant Range Beds|64971|6|Mentioned|p684|||Superseded now by Grant Group.||||||09-FEB-10
75239|Grant Range Beds|66949|6|Mentioned|p9|||Woolnough (1933). Subsequently Grant Formation (Guppy et al., 1952) and Grant Group (Crowe and Turner, 1976).||||||
77771|Grant Sequence, Lower|64981|6|Mentioned|p670.|||Not a formal name; specifically rejected in this article in favour of dividing the Grant Group into three units: Betty, Winifred and Carolyn Formations.||||||
23635|Grants Patch Group|22534|5|Briefly described|p8, Fig.4 p7|||||||||
23635|Grants Patch Group|22596|6|Mentioned|Fig.9 p419|||||||||
23635|Grants Patch Group|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Ora Banda Domain.||||||07-NOV-08
23635|Grants Patch Group|42221|5|Briefly described|Table 1 P6|||||||||
23635|Grants Patch Group|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
23635|Grants Patch Group|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23635|Grants Patch Group|43101|5|Briefly described|Table 1.|||||||||
23635|Grants Patch Group|43162|6|Mentioned|5|||||||||
23635|Grants Patch Group|43496|6|Mentioned|6|||||||||
23635|Grants Patch Group|50551|5|Briefly described|1095||Archean|In Eastern Goldfields Province.||||||07-NOV-08
23635|Grants Patch Group|60514|5|Briefly described|p61, p64, 65 Table. 1|Archean|Archean|Includes; Victorious Basalt, Bent Tree Basalt,Mt Pleasant Sill, Enterprise Dolerite. High-Mg and tholeiitic basalt; massive, pillowed, and vesicular lavas. Geological Province: Yilgarn Craton.||||||07-FEB-11
23635|Grants Patch Group|60627|5|Briefly described|p61, p65 Tb.1|||Mafic Volcanics.||||||
23635|Grants Patch Group|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Ora Banda domain. Komatiitic and tholeiitic basalt. Includes Victorious Basalt, Bent Tree Basalt, Mount Pleasant Sill and Mount Ellis Sill.||||||11-JUN-15
23635|Grants Patch Group|65834|6|Mentioned|p7, 37|||Ora Banda Domain, Kalgoorlie Terrane.|||Victorious, Bent Tree Basalts; Mount Pleasant, Mount Ellis Sills.||High Mg and tholeiitic basalt; massive, pillowed and vesicular lavas.|
23635|Grants Patch Group|73391|6|Mentioned|p203, 278, 310, Appendices.|||Witt (1990). Mount Pleasant, Ora Banda Domain.|||Victorious, Bent Tree Basalts.|||
83146|Grass Flats gabbro|72491|6|Mentioned|p5 Fig.4|||Southern Cross Terrane, Yilgarn Craton.||||||
35668|Grave Dam Grit|23142|5|Briefly described|p203 Fig.2|||||||||
35668|Grave Dam Grit|60514|6|Mentioned|p48 Fig. 2|Archean|Archean|Angular felsic rudite. Geological Province: Yilgarn Craton.||||||07-FEB-11
35668|Grave Dam Grit|60625|5|Briefly described|p48 Figs. 1,2|||Angular felsic rudite. Geological Province: Eastern Goldfields.||||||
35668|Grave Dam Grit|63637|6|Mentioned|p5 Fig. 1.2, p10|||A name which may eventually be abandoned due to changed interpretation of its lithology (p10). Interpreted to lie (dis)conformably over Kanowna Conglomerate. Geological province: Eastern Goldfields Province||||||17-OCT-07
35668|Grave Dam Grit|70482|5|Briefly described|p319, 323-324|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Very thick: 1500m?|2667 +/- 10 Ma (MDA: Tripp et al., 2007).|Kalgoorlie Sequence.||(Dis)conformably overlies Kanowna turbidite.|Strongly to intensely altered unit interpreted to contain abundant quartz and feldspar crystals (products of a pyroclastic flow deposit/ignimbrite).|
35668|Grave Dam Grit|71166|6|Mentioned|p22, p24 fig 3.17.||||||||Moderately to well-sorted, poorly bedded sandstone and grit.|
35668|Grave Dam Grit|72049|5|Briefly described|p256|||Geochronology analyses, results, and interpretation are discussed in detail. Spread up to ~2724 Ma; sub-pop. ~2668 Ma; 1 older grain ~2636 Ma; (n = 32) U-Pb SHRIMP dating(Ross et al. 2004).||Black Flag Group ?||||18-MAR-19
35668|Grave Dam Grit|73391|4|Described|vii, 26, 51, 157-159, 168, 188, 222-224|||See also p241, 419-420, 442, Appendices. Also appears as Grave Dam grit (p154, 157, 306), Grave Dam Member (p154), Grave Dam member (p132, 143, 148, 153-160, 166, 174, 177-178, 182-183, 194, 196, 239, 244, 247, 307, 315, 317-318, 416, 444) and even Grave Dam Formation (p155). The Grave Dam sequence at Kanowna is dated at 2668 +/- 10 Ma.|2667 +/- 10 Ma (MDA).|Gidji Lake Formation.||Overlies Kanowna and Ballarat Conglomerates. Is overlain unconformably by Panglo member.|Sandstone, dacitic volcaniclastic rocks. Has basal quartz-rich siltstone in several drill hole intersections; fine lithic wacke in others.|
80209|Grave Dam member|71166|5|Briefly described|p23|||[An informal, probable company name from the Kanowna gold camp]|||||Polymictic volcaniclastic conglomerate, breccia and sandstone.|
80209|Grave Dam member|73391|4|Described|p132, 143, 148, 153-160, 166, 174|||See also p177-178, 182-183, 194, 196, 239, 244, 247, 307, 315, 317-318, 416, 444. Kanowna district. Estimated thickness 1700m. Appears as Grave Dam Member on p154. See also Grave Dam Grit (vii, 26, 51, 157-159, 168, 188, 222-224, 241, 419-420, 442, Appendices). Detailed description: stratigraphic column, photographs. Correlated with Upper Black Flag Formation.|2668 +/- 10 Ma (MDA: Ross et al., 2004).|Black Flag Formation.||Overlies Golden Valley member and, unconformably, Kanowna, Government Dam and Ballarat members. Is overlain unconformably by Panglo member or Government Dam member.|Thickly-bedded felsic, locally polymictic, volcaniclastic breccia interbedded with feldspathic sandstone and polymictic conglomerate. Rare intercalated mafic volcanic units. Intruded by hornblende-feldspar porphyry dykes and sills.|
77549|Gravedam Grit|66880|6|Mentioned|p13. |Archean|Archean|This correlates with a sample of volcanigenic sandstone with a maximum depositional age of 2682 +/- 13 Ma.|2682 +/- 13 Ma.|||||01-NOV-12
83853|Graves Dam Grits|65834|5|Briefly described|p36|||Kanowna Belle gold mine, Boorara Domain, Kalgoorlie Terrane. Mine terminology.||||Locally grades into QED Rudite. Is intruded by Kanowna Belle Porphyry.|A quartz-rich pebbly-grit unit.|
25029|Grebe Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Eocene|Paleocene|In figure, Fm = Formation. Geological Province: Bonaparte Basin. Medium to coarse-grained, well sorted, friable sandstones interbedded with calcarenite and minor calcilutite.||||||01-MAR-10
25029|Grebe Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Paleogene|Browse Basin.||||Overlies Bassett Formation. Is overlain by Cartier Formation.||18-SEP-14
25029|Grebe Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|Name changed to Grebe Sandstone Member (of Hibernia Formation).||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
25029|Grebe Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Palaeogene|Unit of Woodbine Group. Overlies Bassett Formation and underlies Cartier Formation.||83||||28-OCT-14
25029|Grebe Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Eocene|Of the Woodbine Group.||||||01-MAR-10
25029|Grebe Formation|23377|4|Described|p212 Fig.5||Tertiary|||||||
25029|Grebe Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
25029|Grebe Formation|24218|5|Briefly described|p850|Early Eocene|Early Eocene|Geological Province: Bonaparte Basin.||||||
25029|Grebe Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25029|Grebe Formation|42066|5|Briefly described|Fig.3 P199|||||||||
25029|Grebe Formation|60634|6|Mentioned|p1167 Fig.2,  p1168 Fig.3.|Eocene|Eocene|||Unit in Woodbine Group.||Overlies Johnson Formation. Is overlain by Hibernia Formation.||
25029|Grebe Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Johnson Formation. Is overlain by Hibernia Formation.||
25029|Grebe Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Both Grebe Marl and Grebe Formation names are used on this chart.  Age: ~55-~51Ma. Geological Province: Vulcan Sub-basin, Londonderry High and Northern Bonaparte Basin.||||||01-MAR-10
25029|Grebe Formation|63358|5|Briefly described|p4 Fig. 1.3|Oligocene|Eocene|||||||01-MAR-10
25029|Grebe Formation|64689|5|Briefly described|p13 Fig. 13, p16 Fig. 17|Eocene|Eocene|Cartier Trough. Lowstand basin floor facies. May form a stratigraphic trap for Jurassic oil migrating up fault conduits.||||||
25029|Grebe Formation|64695|5|Briefly described|p262 Fig.8|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Johnson Formation. Is overlain by Hibernia Formation.||
25029|Grebe Formation|64697|5|Briefly described|p84 Fig.2, p86, p87 |Eocene|Eocene|||||||
25029|Grebe Formation|66187|5|Briefly described|p413 Fig.2|Eocene||Unit in Woodbine Group. Underlies the Hibernia Formation, overlies the Johnson Formation. Mount Ashmore Dome.||||||
25029|Grebe Formation|68223|6|Mentioned|p179 Fig.4|Eocene|Eocene|||||||
72631|Grebe Marl|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Both Grebe Marl and Grebe Formation names are used on this chart.  Age: ~55-~51Ma. Geological Province: Ashmore Platform.||||||
39318|Grebe Sands|24429|5|Briefly described|p37|Eocene|Eocene|||||||
38086|Green Hole Beds|23570|6|Mentioned|p235 Appendix 1|||||||||
28587|Green Hole Conglomerate|23570|4|Described|p233 Appendix 1|||Name possibly should be abandoned due to lack of definition.  Max. thickness: up to 335m.||||||
28587|Green Hole Conglomerate|36882|6|Mentioned|p124|||||||||
28587|Green Hole Conglomerate|39444|6|Mentioned|Table 4|||||||||
28587|Green Hole Conglomerate|39697|6|Mentioned|p118|||||||||
28587|Green Hole Conglomerate|41635|6|Mentioned|p23|||||||||
28587|Green Hole Conglomerate|45923|4|Described|p.81||Neoproterozoic|On many pages 66, 67, 82, 91, map SF51-5.  See also Green Hole Conglomerate formation, p.82.||||||
28587|Green Hole Conglomerate|67229|6|Mentioned|p3 Fig.2|||Noldart and Wyatt (1962). Obsolete name: rocks included in the Hardey Sandstone.||||||
32729|Green Hole beds|45923|14|Not recorded|p81|||||||||
38084|Green Hole conglomerate|23570|6|Mentioned|p233 Appendix 1|||Misspelt  - see Green Hole Conglomerate.||||||
81376|Greenfields Sill|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Black Flag Group. Correlable to Ora Banda Sill and Turret Dolerite.||
81376|Greenfields Sill|73391|6|Mentioned|Appendices.|||Standing and Castleden (2002). Regional stratigraphic correlation chart of other workers.||||||
81377|Greenmont Sill|70326|5|Briefly described|p360,363|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Intruded into Brilliant Ultramafic.||
75101|Greenmount Granite|64769|6|Mentioned|p31 Tb. 4, p33|||Light-medium grey and medium-grained granite. WA.||||||16-APR-09
31938|Greenough sandstone|43876|14|Not recorded|p581||Early Jurassic|||||||
77529|Greenstone Sequence, Lower|66880|6|Mentioned|p8-9.|Archean|Archean|Northern Yandal Greenstone Belt., western margin.|||||Mafic and ultramafic rocks with chert and banded iron formation.|01-NOV-12
77530|Greenstone Sequence, Middle|66880|5|Briefly described|p8, p26. |Archean|Archean|Northern Yandal Greenstone Belt. Well-represented by the Jundee Mine Sequence. Dacitic volcanics aged 2673 +/- 5 Ma are same age as Kalgoorlie Sequence.|Between c.2678 Ma and c. 2660 Ma.||||Basalt, high MgO basalt, black shale, ultramafic rocks, dolerite sills, locally abundant felsic volcanic and subvolcanic rocks.|
77531|Greenstone Sequence, Upper|66880|5|Briefly described|p8. |Archean|Archean|Northern Yandal Greenstone Belt.|Between c.2678 Ma and c. 2660 Ma.||||A thick sequence of felsic volcanic and sedimentary rocks, with minor chert, shale and dolerite.|
41865|Gregory Granite Complex|50544|6|Mentioned|p43|||Misspelt - intended as Gregory Granitic Complex.||||||
41865|Gregory Granite Complex|64943|5|Briefly described|p27 Table 5|Mesoproterozoic||Unconformably underlying Tarcunyah Group. Metamorphic biotite dated at ~1200 Ma||||||
41865|Gregory Granite Complex|67202|5|Briefly described|p222, p233, p235-237|||Mount Gregory area, Pilbara Craton. Has U contents of 7ppm or more.||||Is overlain unconformably by Googhenama Formation (Tarcunyah Group).|Includes metamorphosed dolerite and gabbro, amphibolites, metamorphosed ultramafic rocks and calc-chlorite-tremolite-serpentine assemblages.|
28588|Gregory Granitic Complex|22475|5|Briefly described|p495|Archean|Archean|||||||07-NOV-08
28588|Gregory Granitic Complex|22716|6|Mentioned|table4, p230|Archean|Archean|||||||07-NOV-08
28588|Gregory Granitic Complex|22953|6|Mentioned|Fig1p3|||||||||
28588|Gregory Granitic Complex|23570|6|Mentioned|p18|||Geological Province: Pilbara Craton||||||
28588|Gregory Granitic Complex|23575|5|Briefly described|Map Legend|||Geological Province Hamersley Basin.||||||
28588|Gregory Granitic Complex|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlying unit Hardey Formation. Underlying unit Mount Roe Basalt. Geological Province Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|23585|4|Described|p13|Archean|Archean|Age: c.2764-2757 Ma (U-Pb zircon). Overlying unit Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|23590|5|Briefly described|p6|Archean|Archean|Overlying unit Tarcunyah Group.||||||07-NOV-08
28588|Gregory Granitic Complex|23594|3|Fully described|p7|Archean|Archean|Age: c.2760 Ma. Overlying unit Koongaling Volcanic Member. Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|23745|4|Described|p8|Archean|Archean|Age: c.2760 Ma. Alkaline A-type felsic igneous rocks. Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|23746|4|Described|p7|Archean|Archean|Age: c.2760 Ma. Formerly Gregory Range Granite. Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|24025|4|Described|p13|Archean|Archean|Of Mount Bruce Supergroup.  Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
28588|Gregory Granitic Complex|30484|6|Mentioned|p56|||Re age dates. Variation of Gregory Range?||||||
28588|Gregory Granitic Complex|37212|6|Mentioned|p5|||||||||
28588|Gregory Granitic Complex|38768|6|Mentioned|p81|||||||||
28588|Gregory Granitic Complex|39426|6|Mentioned|p8|||||||||
28588|Gregory Granitic Complex|39697|3|Fully described|p50|||See also p172.||||||23-OCT-15
28588|Gregory Granitic Complex|41669|3|Fully described|p16|||||||||
28588|Gregory Granitic Complex|42278|6|Mentioned|p33|||||||||
28588|Gregory Granitic Complex|42352|5|Briefly described|p9, p31|||||||||
28588|Gregory Granitic Complex|42785|6|Mentioned|p271|||||||||
28588|Gregory Granitic Complex|43055|5|Briefly described|p11|||||||||
28588|Gregory Granitic Complex|44111|6|Mentioned|p.59|||Probable age for uplift c.1200 Ma.||||||
28588|Gregory Granitic Complex|44152|5|Briefly described|p177|||Of Hickman (1983; see also 1978). Includes also gneiss and granite to S, and his Ragged Hills Granophyre.|||||Granophyre, gneiss, granite.|23-OCT-15
28588|Gregory Granitic Complex|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
28588|Gregory Granitic Complex|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28588|Gregory Granitic Complex|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28588|Gregory Granitic Complex|50544|3|Fully described|p42, p10 Fig. 5|Archean|Archean|Of the Mount Bruce Supergroup.  Granophyre is the main component on YARRIE.  Underlies the Koongaling Volcanic Member (Hardey Formation).  Age: c.2764-2757Ma.  Geological Province: Hamersley Basin (Gregory Range Inlier).||||||01-FEB-17
28588|Gregory Granitic Complex|50555|5|Briefly described|Map legend|Archean|Archean|Age: c. 2761-2557Ma.   Geological Province: Hamersley Basin.||||||07-NOV-08
28588|Gregory Granitic Complex|60373|5|Briefly described|p150 Tb. 2|Archean|Archean|Ages: 2757+/-5, 2761+/-2, 2762+/-4, 2763+/-8 (SHRIMP, Nelson 1996).||||||
28588|Gregory Granitic Complex|65403|6|Mentioned|p14.|Archean|Archean|||||Is overlain unconformably by Tarcunyah Group.||
28588|Gregory Granitic Complex|65725|5|Briefly described|Map legend|Neoarchean|Neoarchean|Undivided granitoid. 2763-2757 Ma. Province: Pilbara Craton||||||
28588|Gregory Granitic Complex|65827|5|Briefly described|p32|Neoarchean|Neoarchean|2766-2757 Ma; coeval with Bamboo Creek Member. Comagmatic with Koongaling Volcanic Member.
||||||21-MAY-14
28588|Gregory Granitic Complex|67183|5|Briefly described|p640-641, p647, p648, p656 Fig.15, p671|Neoarchean|Neoarchean|Marks the edge of the Pilbara Craton.||||Correlates with the Collier Subgroup. Unconformably overlain by Googhenama Formation.||
28588|Gregory Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
28588|Gregory Granitic Complex|71042|6|Mentioned|p69|||||||||
38543|Gregory Range granitoids|23813|6|Mentioned|p90 Tb. 1|Archean|Archean|Informal name.  Geological Province: Pilbara Craton.||||||07-NOV-08
38543|Gregory Range granitoids|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.2.76-2.69 Ga. Geological Province: Pilbara Craton. Of the Fortescue Group.||||||07-NOV-08
32597|Gregory Range members|45923|14|Not recorded|p.80|||||||||
25033|Guildford Clay|12759|1|Redefined|p43-7; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined Aurousseau and Budge (1921) as "Guildford Clays".; rdefined as a Formation by Low (1971); eedefined here as Guildford Clay. Max thickness up to 35 m. Type area in Swan River Valley around Guildford.||Of Kwinana Group.||Unconformably overlies Ascot, Yoganup or Kings Park Formations. Interfingers with Gnangara and Bassendean Sands.|Predominantly brown silty and slightly sandy clay with subordinate lenses of sand and gravel. Predominantly fluvial.|12-MAY-14
25033|Guildford Clay|24464|5|Briefly described|p332 Fig. 1|||||||||
25033|Guildford Clay|31896|6|Mentioned|p34|||Renamed Guildford Fm.||||||
25033|Guildford Clay|36257|6|Mentioned|Table 2.1|||||||||
25033|Guildford Clay|43347|6|Mentioned|10|||||||||
25033|Guildford Clay|63745|6|Mentioned|p63|||||||||07-FEB-11
74723|Gunanya Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group. Misspelling of Gunanya Sandstone.||||||
74723|Gunanya Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
25937|Gundockerta Formation|29784|6|Mentioned|Table 1|||||||||
25937|Gundockerta Formation|30900|5|Briefly described|p67|||Table 1||||||
25937|Gundockerta Formation|30956|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25937|Gundockerta Formation|30965|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25937|Gundockerta Formation|31091|6|Mentioned|Fig. 2|||Also mention Fig. 3||||||
25937|Gundockerta Formation|32268|6|Mentioned|Fig. 1|||||||||
25937|Gundockerta Formation|32377|6|Mentioned|p229|||||||||
25937|Gundockerta Formation|32694|6|Mentioned|p1093|||Refers Williams (1970)||||||
25937|Gundockerta Formation|33446|6|Mentioned|p15|||||||||
25937|Gundockerta Formation|33837|5|Briefly described|p167|||Archaean||||||
25937|Gundockerta Formation|33847|2|Defined|p17|Archean|Archean|See also Table 4. c 2615my.||||||07-NOV-08
25937|Gundockerta Formation|33850|4|Described|Table 2|||||||||
25937|Gundockerta Formation|35059|6|Mentioned|p205|||||||||
25937|Gundockerta Formation|36869|4|Described|p46|||||||||
25937|Gundockerta Formation|37004|6|Mentioned|p288|||||||||
25937|Gundockerta Formation|41066|6|Mentioned|1 of 2 M15|||||||||
25937|Gundockerta Formation|41594|5|Briefly described|p41|||||||||
25937|Gundockerta Formation|42892|5|Briefly described|Table 3|||||||||
25937|Gundockerta Formation|43293|5|Briefly described|p3||Archean|||||||07-NOV-08
25937|Gundockerta Formation|44149|5|Briefly described|p91 Tb.2-9|Archean|Archean|Kurnalpi-Edjudina area, Eastern Goldfields Province.|||||Sandstone, conglomerate, acid volcanics.|
25937|Gundockerta Formation|64775|6|Mentioned|p9-9|||Felsic volcanic-epiclastic rocks.||||||
25937|Gundockerta Formation|73391|6|Mentioned|Appendices.|||Williams (1969). Regional stratigraphic correlation chart of other workers.|||||Turbidite sequence, clastic sequence, conglomerate and sandstone.|
25036|Gundockerta Group|37373|5|Briefly described|Table 2.I|||||||||
25036|Gundockerta Group|39869|6|Mentioned|Fig.2|||||||||
25036|Gundockerta Group|41249|5|Briefly described|Table 1|||Mention p19.||||||20-NOV-08
25036|Gundockerta Group|43075|5|Briefly described|Table 1|||||||||
25036|Gundockerta Group|73391|6|Mentioned|p50|||Gemuts and Theron (1975).||||||
33028|Gurabi Formation|44397|14|Not recorded|p.20,22 Table 2||Adelaidean|Louisa Downs Group.||||||
73378|Guran Gutta granite|66299|6|Mentioned|p331.|||Superseded by Gurun Gutta granite.||||||
79234|Gurgdi Basalt|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. [Mis-spelling of Gurgadi].||Cassidy Group.||Overlies Gombugurra Rhyolite. Is overlain by Thomas Rhyolite.|Basalt with vesicular and amygdaloidal flow tops; epidotised.|
42480|Gurun Gutta granite|50216|5|Briefly described|p213|Paleoproterozoic|Paleoproterozoic|Of the northern Gascoyne Complex. Age: 1652+/-5 Ma (Culver, 2001).||||||07-NOV-08
42480|Gurun Gutta granite|63246|6|Mentioned|p481, p490|Neoproterozoic|Neoproterozoic|See also the informal "Gurun Gutta granite". Age: 1652+/-5Ma (U-Pb zircon). In spite of these zircons' age, it's magmatic age is interpreted to be between 990 and 950Ma in this study.||||||13-NOV-15
42480|Gurun Gutta granite|64872|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Informal name. An undeformed leucocratic, tourmaline-bearing granite pluton intruding Pooranoo Metamorphics. Monazite (SHRIMP) age of c. 870 Ma interpreted as crystallisation age.|c. 870 Ma.|||||16-MAR-12
42480|Gurun Gutta granite|66299|5|Briefly described|p15, p331.|||Undeformed, post-Edmundian Orogeny intrusion. Typically leucocratic; locally tourmaline-rich.|Low Zr; age of xenocrystic zircons 1652 +/- 4 Ma.|||||
73381|Gurun Gutta granite""|63246|5|Briefly described|p478, p481|||Informal - see also Gurun Gutta granite. Age: c.1650Ma (SHRIMP U-Pb zircon: Virvell 2001). Undeformed leucocratic granite that intrudes schists in the Gascoyne Complex; cuts across Pooranoo and Morrissey Metamorphics. See also p491.||||||31-MAY-07
73381|Gurun Gutta granite""|66241|5|Briefly described|p10.|Neoproterozoic|Neoproterozoic|Gascoyne Province. Undeformed. Cuts the Edmundian Orogeny (1030 - 950 Ma) fabrics in the northern Mutherbukin zone.|c.910 Ma (Johnson et al. 2009).|||||
41046|Gwalia slate|24196|6|Mentioned|p69 Fig.10|||Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||
70219|Gwna Group|61579|6|Mentioned|p77|Proterozoic|Proterozoic|Unclear if an Australian unit or if being used for comparison?  Includes hydrothermal cherts. ||||||
74059|H4 Member|13242|5|Briefly described|p214 Fig. 2|Late Permian|Late Permian|Informal name of Bhatia et al (1984). Member of former Hyland Bay Fm; overlay the former Hay Member, underlay the former Tern Member. Superseded by Dombey Member of former Hyland Bay Fm, Kinmore Group (Mory, 1988, 1991). Geol.Prov: Bonaparte Basin.||||||07-FEB-11
74060|H5 Member|13242|5|Briefly described|p214 Fig. 2|Late Permian|Late Permian|Informal name (Bhatia et al 1984). Of former Hyland Bay Fm; overlay the informally named Basal Mbr, underlay Hay Mbr. Renamed Pearce Mbr and overlies the now unnamed basal layer of Hyland Bay Fm, Kinmore Group (Mory 1988, 1991). Bonaparte Basin.||||||07-FEB-11
81858|Haig Conglomerate|70772|6|Mentioned|p33 Table 2, p39|||p39 explains that the Haig Cglm. shown in Table 2 from well HDDH001 is actually Shanes Dam Conglomerate.||||||06-MAY-20
34411|Halls Creek Group, lower|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1880Ma||||||
34412|Halls Creek Group, upper|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|Age: 1855Ma. Formed in submarine fan environment.||||||
67830|Hamelin Formation|1943|4|Described|p383-388, p373, p375 Fig. 3, p376 Fig. 4|Pridoli|Gorstian|New name. Type section in Hamelin Pool-1, 951-1225m. Reference section in Yaringa-1. Shallow marine environment. Conodont fauna not diverse, but give likely early Gorstian to earliest Pridoli age. Divided into lower and upper parts. Max. thickness: 335.5m in Pendock-1A (1856-2191.5m)||Dirk Hartog Group||Overlies Yaringa Evaporite with transitional contact. Is overlain unconformably by Faure Formation, or Nannyarra Formation.||20-JUN-13
67830|Hamelin Formation|6943|6|Mentioned|p601.|||Gorter et al. (1994). Name replaced by Coburn Formation (Mory et al. 1998), including same type section except evaporitic part, named Yaringa Formation.||||||
67830|Hamelin Formation|12729|6|Mentioned|p10.|||Of Gorter et al. (1994). Name replaced by Coburn Formation, since the name Hamelin was previously used for a local Quaternary unit.||||||
67830|Hamelin Formation|13996|6|Mentioned|p148|Ludlow|Ludlow|Microvertebrate remains: species listed.||||||
67830|Hamelin Formation|23935|6|Mentioned|p19|||Superseded by the Coburn Formation. Geological Province: Southern Carnarvon Basin.||||||
38676|Hamelin granite|23788|5|Briefly described|p8|||Informal unit of the Leeuwin Complex. Geological Province: Yilgarn Craton.||||||20-NOV-08
77175|Hamersley BIFs|67829|5|Briefly described|p447.|||Some (if not all) high-grade micro-platy hematite enrichment occurred prior to deposition of overlying unit. Laminated, deep-water deposits. ||||||
30210|Hamersley Formation|43115|6|Mentioned|p178|||||||||
40200|Hamersley Iron Formation|24203|5|Briefly described|p292|Proterozoic|Proterozoic|||||||10-SEP-12
38694|Hamersley Supergroup|23789|5|Briefly described|p30 Fig. 11|Proterozoic|Archean|||||||07-NOV-08
38694|Hamersley Supergroup|60112|6|Mentioned|p106.|||Included in the definition of greenstones as 'any supracrustal sequence in which volcanic rocks occur'.||||||
38694|Hamersley Supergroup|68141|6|Mentioned|p191|Archean|Archean|Pilbara Craton.||||||
37200|Hamersley Surface""|23793|6|Mentioned|p5|||Geological Province: Pilbara Craton||||||
68725|Hamersley shales|60706|6|Mentioned|p624|||Informal - see the Hamersley Group||||||
28594|Hammersley Group|30363|6|Mentioned|p10|||||||||
28594|Hammersley Group|36842|6|Mentioned|p218|||||||||
28594|Hammersley Group|41667|6|Mentioned|p5|||||||||
28594|Hammersley Group|45965|14|Not recorded|p.58,61,64|||||||||
25042|Hampton Conglomerate""|30012|6|Mentioned|p18|||||||||
25042|Hampton Conglomerate""|30563|6|Mentioned|p11|||Refers Fairbridge (1953)||||||
25042|Hampton Conglomerate""|30564|6|Mentioned|p11|||Refers Fairbridge (1953), Lowry (1968).||||||
25042|Hampton Conglomerate""|31904|6|Mentioned|p7|||Refers Fairbridge (1953)||||||
25042|Hampton Conglomerate""|31906|6|Mentioned|p7|||Refers Fairbridge (1953). Now Hampton Sst.||||||
25042|Hampton Conglomerate""|31907|6|Mentioned|p7|||Refers Previous authors. Now Hampton Sst.||||||
25042|Hampton Conglomerate""|31908|6|Mentioned|p7|||Refers Fairbridge (1953)||||||
25042|Hampton Conglomerate""|31913|6|Mentioned|p10|||Refers Fairbridge (1953),Lowry (1968)||||||
25042|Hampton Conglomerate""|32552|6|Mentioned|p50|||See also P56. Refers Fairbridge (1953)||||||
25042|Hampton Conglomerate""|33589|6|Mentioned|p10|||Refers Fairbridge (1953). & Lowry (1968).||||||
25042|Hampton Conglomerate""|35496|6|Mentioned|p21|||Amended to Hampton Sandstone by Lowry(1968)||||||
25042|Hampton Conglomerate""|36890|6|Mentioned|p413|||Renamed Hampton Sandstone||||||
75625|Hampton Formation (Eucla)|23989|5|Briefly described|p54 Fig. 46|Late Eocene|Early Eocene|Misspelt in figure. See Hampton Sandstone.||||||
28595|Hampton Limestone""|31850|6|Mentioned|p35|||Refers Ludbrook (1954)||||||
38730|Hampton Sandstone, upper|24397|5|Briefly described|p234 Tb. 2|||As used in NE margin of Eucla Basin. Replaced by Khasta Formation.  Geological Province: Eucla Basin.||||||19-FEB-15
38729|Hampton sandstone, upper|24397|6|Mentioned|p244|||Informal - see Hampton Sandstone.  Geological Province: Eucla Basin.||||||
83854|Hampton-Boulder Porphyry|65834|6|Mentioned|p61|||Kalgoorlie district. A local name for a 600m long by 80m thick gold-mineralised body.|||||Quartz-feldspar porphyry; pervasively altered.|
67863|Hanging Wall Basalt, Upper|60076|5|Briefly described|p12 Tb. 2|||Informal name.  Vesicular, tholeiitic basalt, locally schistose.  Max. thickness: 1500m.  Geological Province: Kambalda domain.||||||
79527|Hannan's Lake serpentinite|62083|5|Briefly described|p1014 Fig.6|||Main gold camp: Kalgoorlie.||Kambalda Group|||Ultramafic-mafic volcanic rock.|
40327|Hannon's Lake serpentinite|23924|5|Briefly described|p205|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
82959|Hanns Camp Syenite Complex|73238|5|Briefly described|p17|||Laverton district, Eastern Goldfields Terrane. A >40 km long elongate body.|2664 +/- 2 Ma.||||Syenitic and granitic intrusions.|
41048|Hanns Camp porphyritic syenite|24196|6|Mentioned|p11|||Geological Province: Eastern Goldfields Granite-Greenstone Terrane, Yilgarn Craton.||||||
38668|Hanns Camp syenite|23786|5|Briefly described|p56|||Informal name. Geological Province: Yilgarn Craton.||||||
38668|Hanns Camp syenite|24196|5|Briefly described|p49|Archean|Archean|Informal - see Hanns Camp Syenite. Age: 2664 +/- 2 Ma (Black et al., 2002)||||||07-NOV-08
31904|Hansens Folly Gneiss|24197|5|Briefly described|p102 Tb. 14.1|Neoproterozoic|Neoproterozoic|Of O'Callaghans Supersuite. I-type (granodioritic) ilmenite-bearing Mount Crofton type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
31904|Hansens Folly Gneiss|50436|5|Briefly described|p1.3, Table 1.1|Neoproterozoic|Neoproterozoic|Geological Province: Paterson Orogen. Of the O'Callaghans Supersuite.||||||
41434|Harbutt Leucogneiss|50436|6|Mentioned|p3.13|||||||||
69918|Hardey Formation siltstone|61259|6|Mentioned|p405, p406 -7 Tb. 1|||Informal reference to siltstone of the Hardey Formation. ||||||
69919|Hardey Formation, lower|61259|6|Mentioned|p403|Archean|Archean|Informal - see Hardey Formation.||||||07-NOV-08
73579|Harding Granitic Complex|63441|5|Briefly described|p37|Archean|Archean|Considered likely to include large intrusions of the Maitland River Supersuite; includes the two intrusions Forestier Bay Granodiorite and Mount Gregory Monzodiorite, both of the Orpheus Supersuite.||||||07-FEB-11
73579|Harding Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
73579|Harding Granitic Complex|67201|5|Briefly described|p13 Fig.8, p25, p67|||In northwestern Pilbara Craton.||||Occupies core of anticline in Ruth Well Formation. Underlies Cenozoic deposits of coastal plain (aeromagnetic data indication).||
73579|Harding Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
73579|Harding Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
36850|Harding Granitoid Complex|23484|4|Described|p8 Fig. 4|||||||||
36850|Harding Granitoid Complex|23780|5|Briefly described|p178|Archean|Archean|Age: ~3016+/-4 Ma||||||07-NOV-08
36850|Harding Granitoid Complex|23784|5|Briefly described|p10|Archean|Archean|||||||07-NOV-08
36850|Harding Granitoid Complex|23789|4|Described|p12|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36850|Harding Granitoid Complex|23793|4|Described|p32|Archean|Archean|||||||07-NOV-08
36850|Harding Granitoid Complex|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36850|Harding Granitoid Complex|23813|5|Briefly described|p89|Archean|Archean|Age: 3260Ma. Intrudes the Roebourne Group.  Geological Province: Pilbara Craton.  See also p91 Tb. 1.||||||07-NOV-08
36850|Harding Granitoid Complex|23936|5|Briefly described|Tb.1|Archean|Archean|Age: ca. 3.26 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
36850|Harding Granitoid Complex|24023|5|Briefly described|p23|Archean|Archean|||||||07-NOV-08
36850|Harding Granitoid Complex|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
36850|Harding Granitoid Complex|24184|4|Described|p712, p715 Fig.11|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36850|Harding Granitoid Complex|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Age: ca. 3015 Ma. Geological Province: Mallina basin||||||07-NOV-08
36850|Harding Granitoid Complex|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 3015 Ma||||||07-NOV-08
36850|Harding Granitoid Complex|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Pilbara Craton. Age: 3015-2970 Ma||||||07-NOV-08
36850|Harding Granitoid Complex|24541|5|Briefly described|p17 Tb.4|Archean|Archean|Age: 2970 Ma. Geological Province: West Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
36850|Harding Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||West Pilbara. Poorly exposed.|||||Foliated monzogranite, granodiorite, migmatite; some porphyritic phases.|
36850|Harding Granitoid Complex|50430|5|Briefly described|p164||Archean|3016-2970 Ma. In West  Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
36850|Harding Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane. Isotopic ages (with +/- error) from Nelson, 1997 and Nelson, 1999, respectively.|3015-2970 Ma; 3014 +/- 3 Ma and 2970 +/- 5 Ma |||||
73865|Harding Granitoid-Gneiss Complex|24550|5|Briefly described|p76|Archean|Archean|Same as Harding Granitoid? Contains tonalitic plutons with age of 3014+/-3Ma (Nelson 1997), 3024+/-4 and 3031+/-6Ma (Smith et al 1998).||||||07-FEB-11
39740|Harding granitoid complex|24193|5|Briefly described|p874 Fig. 1, p888|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
72771|Hardy Formation|62986|5|Briefly described|p18|||Of the Fortescue Group. Geological Province: Pilbara Craton.||||||25-JAN-07
25044|Hargreaves Member|32664|6|Mentioned|Map legend|Late Devonian|Late Devonian|Briefly described in notes||||||
25044|Hargreaves Member|32865|6|Mentioned|p468|||Frasnian||||||
25044|Hargreaves Member|36890|4|Described|p376|||||||||
25044|Hargreaves Member|40301|6|Mentioned|p7|||||||||
25044|Hargreaves Member|42994|6|Mentioned|p239|||of Cockatoo Formation||||||
25044|Hargreaves Member|45038|2|Defined|p.17,34||Late Devonian|||||||
25044|Hargreaves Member|45039|6|Mentioned|p7|||See also PP8,18,148. Upper Devonian||||||
25044|Hargreaves Member|45040|14|Not recorded|p5, Fig.2||Late Devonian|(Upper Devonian). Pt. Cockatoo Formation.||||||
25044|Hargreaves Member|45050|6|Mentioned|p33|||See also P44 & Tables 4,7||||||
25044|Hargreaves Member|45063|6|Mentioned|p6|||Frasnian. See also P13, 23 & Fig. 3.||||||
25044|Hargreaves Member|48886|14|Not recorded|Map||Late Devonian|Upper Devonian.||||||
25044|Hargreaves Member|68298|5|Briefly described|p216|||Bonaparte Basin. Limestone horizon||Cockatoo Formation||||
83380|Harper Lagoon Ultramafics|73391|6|Mentioned|p279|||Barrick (2011: unpublished data). Boorara Domain, Kalgoorlie Terrane. 850m thick.||||||
34451|Hart Dolerite sills|22754|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Informal - see Hart Dolerite.  Age: c. 1800Ma (SHRIMP).||||||07-NOV-08
80593|Hart Granophyre|70731|6|Mentioned|p278|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
80593|Hart Granophyre|70851|6|Mentioned|p29 Fig 24|||Invalid name shown in a diagram along with Hart Dolerite.||||||10-AUG-18
25045|Hart Springs Sandstone|41598|6|Mentioned|p412|||||||||
25944|Harvey Beds|33801|6|Mentioned|p52|||||||||
25944|Harvey Beds|36293|2|Defined|p204|early Pleistocene|Tertiary|Tertiary or Early Pleistocene||||||
25944|Harvey Beds|40359|5|Briefly described|p25|||||||||
69662|Harvey beds|61155|5|Briefly described|p17|Late Eocene|Middle Eocene|Geological region: Darling Range. ||||||
80320|Hasties Gabbro|67202|5|Briefly described|p184|Tonian|Tonian|Yeneena Basin. Unclear if this is meant to be a formal name.|837 +/- 6 Ma (Maidment, pers. comm.).|||Correlates with Gairdner Dyke Swarm.||31-JAN-18
39561|Hawker Group sediments|24465|6|Mentioned|p343|||Informal name - see Hawker Group.||||||
81304|Hawkes Nest Supersuite|70020|6|Mentioned|p122|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton. HFSE-enriched granitic supersuite.||||||
73599|Hayes Well Ultramafic Unit|63459|6|Mentioned|p802|Archean|Archean|Of Hunter et al (1994). Local name for ultramafic unit in the wastern part of the ca.2.7Ga  Agnew-Wiluna Greenstone Belt; Airport Ultramafic Unit is in the east. Geological Province: Yilgarn Craton.||||||07-NOV-08
74724|Hazlett beds""|64580|4|Described|map legend||Mesozoic|Sandstone, siltstone, claystone. Eastern Canning Basin.||||||15-DEC-08
37191|Headley Limestone|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Goose Hole Group. Geological Province: Ord Basin.||||||
37191|Headley Limestone|60682|5|Briefly described|p21|||Overlies Antrim Plateau Volcanics.||||||
80321|Heavitree Sandstone|67202|6|Mentioned|p181|||Amadeus Basin.||||Corresponds with Coolbro Sandstone (Yeneena Basin).||
80321|Heavitree Sandstone|72601|6|Mentioned|p7|||Renamed to the Heavitree Formation.||||||
41201|Heines member|50222|6|Mentioned|p327|||Informal - see Heines Member.||||||22-JUN-04
72828|Heins Member|49896|5|Briefly described|p3 Tb. 2|||Probably misspelt? Of the Wilthorpe Formation. Polymictic conglomerates. See also Heines Member. ||||||
25945|Helena Creek Beds|24197|5|Briefly described|p81|Paleoproterozoic|Paleoproterozoic|Of the Tanami Complex. Geological province: The Granites-Tanami Block.||||||07-FEB-11
25945|Helena Creek Beds|29804|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25945|Helena Creek Beds|29805|4|Described|Table 1|||||||||
25945|Helena Creek Beds|29809|6|Mentioned|Table 1|||||||||
25945|Helena Creek Beds|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25945|Helena Creek Beds|42504|5|Briefly described|Table 3 P60|||||||||
25945|Helena Creek Beds|45140|2|Defined|p13-15, p18-19, p23, Appx.p5|Paleoproterozoic|Paleoproterozoic|Blake et al. (1975). Named after Helena Creek. The Granites-Tanami Block; NW of Winnecke Range. The reference area is 35km E of Nongra Lake, between points 18deg 16'30"S 130deg 08'00"E, 18deg 16'20"S 130deg 10'00"E and 18deg 18'00"S 130deg 09'00"E. Probably over 1000m thick. Metamorphism, structure described.||Tanami Complex.||Is overlain unconformably by Antrim Plateau Volcanics. Is intruded by Winnecke Granophyre.|Lithic arenite, greywacke, conglomerate and phyllitic mudstone. Local thin-bedded to laminated grey tuff and acid porphyry in the SE, and massive maroon, fine-grained and iron-stained tuff and quartzitic hornfels in the SW.|
25945|Helena Creek Beds|46864|6|Mentioned|p37|||||||||
25945|Helena Creek Beds|48950|2|Defined|p20|Archean|Archean|||||||07-NOV-08
25945|Helena Creek Beds|50589|5|Briefly described|p1.1|||Geological Province: Granites-Tanami Block. Of the Tanami Complex. Intruded by: The Granites Supersuite.||||||
25945|Helena Creek Beds|69426|5|Briefly described|p11:5 Fig.11.4, 11:7|||Blake et al. (1975). Later incorporated into the Mount Winnecke Formation. Also appears as Helena Creek beds on p11:7, [mistakenly] attributed to Blake et al. (1975).||||Overlain by Pargee Sandstone.||12-JUL-16
25945|Helena Creek Beds|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1842+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Arenite.|
78077|Henley Sandstone|68254|6|Mentioned|p1036 Fig.2|Cretaceous|Cretaceous|Presented as Henley Sandstone. See Henley Sandstone Member in this paper.||||||
25054|Herschell Limestone|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||24-NOV-09
25054|Herschell Limestone|32645|6|Mentioned|Map legend|Holocene|Holocene|||||||
25054|Herschell Limestone|35093|3|Fully described|p17|||||||||
25054|Herschell Limestone|37017|6|Mentioned|Map legend|Recent|Recent|||||||
25054|Herschell Limestone|41831|4|Described|p557|||||||||
25054|Herschell Limestone|43297|6|Mentioned|p18|||Rottnest Island.||||||
25054|Herschell Limestone|43310|5|Briefly described|Map Legend||Quaternary|||||||
25054|Herschell Limestone|43495|6|Mentioned|20|||||||||
25054|Herschell Limestone|43504|6|Mentioned|14||Quaternary|||||||
25054|Herschell Limestone|44144|4|Described|p501 Tb.4-21|Holocene|Holocene|Type Section: SW of Mount Herschell 31o59'45''S 115o31'30''E.  3m thick.||Kwinana Group||Overlies Tamala Limestone disconformably.|Weakly lithified coquinite, lime sand, marl.|
25054|Herschell Limestone|63807|4|Described|p10-11|Recent|Holocene|Age is Middle Holocene to modern. Overlies and abuts the Tamala Limestone. Thickness: >3m. Shell beds, sand dunes, beach sand, swamp deposits and lake deposits; mainly shelly beds with intercalated lime sand and marl.||||||17-MAY-21
25054|Herschell Limestone|68811|5|Briefly described|p73|||Poor aquifer properties. |||||Shell beds, lime sand and clay.|
25054|Herschell Limestone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||marine sediment|
25054|Herschell Limestone|71958|5|Briefly described|p35|Holocene|Holocene|Vlaming Sub-basin. Exposed in outcrops on the Rottnest islands where it occurs adjacent to prominent saline lakes.|||||Fossiliferous calcarenite and marl.|
69653|Hibernia Formation""|61155|5|Briefly described|p15|Late Eocene||Informal variation on Hibernia Formation. Max. thickness: 1200m in Sahul Platform region. Geological Province: Bonaparte Basin / Ashmore and Sahul Platforms, Vulcan and Petrel Sub-basins. ||||||
34224|Hibernia Sandstone|22663|5|Briefly described|AC97 1-4 Fig.4||Oligocene|||||||
32793|High Cliff Formation|44237|14|Not recorded|Fig.2||Permian|||||||
32793|High Cliff Formation|48857|14|Not recorded|p.18|||||||||
33014|High River Shale|44395|14|Not recorded|p.8|||Of Pertaoorrta Group; correlates with the Cleland Sandstone.||||||
75367|Highcliff Sandstone|14227|5|Briefly described|p10, Enclos. 2|Sakmarian|Sakmarian|Also presented as High Cliff Sandstone - both forms of the name used interchangeably. Glacio-marine sands. Geol. Prov: Perth Basin.||||||07-FEB-11
42464|Highland Bay Formation|60701|6|Mentioned|p13|||Misspelt - see Hyland Bay Formation.||||||
83381|Highway Ultramafic|73391|6|Mentioned|p194, 244|||Boorara Domain, Kalgoorlie Terrane.|2708 Ma.|||Overlies Big Blow Chert. Is overlain by Upper Basalt.||
69189|Highway ultramafics|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Informal name. Underlain by Scotia Basalt. Geological Province: Boorara Domain, Yilgarn Craton.||||||07-FEB-11
69189|Highway ultramafics|60627|5|Briefly described|p65 Tb.1|||Informal name||||||
38968|Hilly Basalts|23807|6|Mentioned|p133|||Geological Province: Pilbara Craton.||||||
68145|Hiltaba Suite Granites|67621|6|Mentioned|p212|||Gawler Craton.||||||
68146|Hiltaba Suite Granitoids|67028|5|Briefly described|p361-362, p367, p372-3|Calymmian|Calymmian|Gawler Craton. Information on magnetic characteristics presented. Age from Fanning et al. (1988). Includes both A-type and I-type volcanics. Roxby Downs-type are oxidised, fractionated with hematite dusting of feldspar; Kokatha-type are reduced, containing pyrite.|1595 - 1575 Ma||Charleston Granite, Cunyarie Rocks Granite, Buckleboo Granite.|Co-magmatic with Gawler Range Volcanics, and also intrudes them at ~1575 Ma.||24-APR-12
69745|Hinckley Range Gabbronorite|61340|5|Briefly described|Map legend|||Presented as the compound name Hinckley Range Gabbronorite/Troctolite Intrusion.||||||21-SEP-05
69746|Hinckley Range Troctolite|61340|5|Briefly described|Map legend|||Presented as the compound name Hinckley Range Gabbronorite/Troctolite Intrusion.||||||
41367|Hinckley Range gabbronorite|44109|4|Described|p14, p151|Mesoproterozoic|Mesoproterozoic|Informal name. See also Hinckley Range gabbronorite intrusion. Mafic granulite; granite-veined mafic granulite that envelopes bodies of gabbro, amphibolite and foliated granite. Within the Giles Complex. ||||||
41367|Hinckley Range gabbronorite|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Giles Complex.||||||
69753|Hinckley Range gabbronorite intrusion|44109|4|Described|p9, p60|Mesoproterozoic|Mesoproterozoic|Informal part of Giles Complex. Gabbroic with common cumulates being gabbroic troctolite, troctolitic gabbro, gabbronorite, anorthosite and minor pyroxenite. Max. thickness: 5800m. ||||||
69753|Hinckley Range gabbronorite intrusion|61339|5|Briefly described|Map legend|||Informal name.  Thickness: <6000m.||||||21-SEP-05
70169|Hinckley Range granites|44109|6|Mentioned|p110|Mesoproterozoic|Mesoproterozoic|Informal reference to the gabbronorite of the Hinckley Range intrusion. ||||||
78330|Hinckley Range intrusion|65135|5|Briefly described|p16, p17|||Informal name. Of the layered Giles intrusions. Cross-cut by Gairdner dykes.||||||
79624|Hinckley gabbro|68996|5|Briefly described|p5, p50, p51, p52 Table 7, p68|Mesoproterozoic|Mesoproterozoic|Also Hinkley intrusion p47,p52, 68. Part of G1 group. Connected to Wingellina Hills intrusion. ||Giles Suite||||
28071|Hinkley Gabbro|69153|5|Briefly described|GA_geochron.csv|||Misspelt. See also Hinckley Range Gabbro. 3 samples recorded: 1. metabasite -- Data migrated from OZCHRON1. Original comment: 'This sample is either a chilled phase of Hinckley Range gabbronorite or a type A dyke. The anhedral zircons have igneous zonation, and this magmatic crystallisation age is based on 6 grains only. Age consistent with best age of Giles Complex (1078+/-3 Ma)'; 2. felsic intrusive -- Foliated granite dyke, Champ de Mars, Tomkinson Ranges, Western Musgrave Block. Sun, S.S. Gray, C.M. Sheraton, J.W. 1995. Zircon U-Pb chronology and neodymium isotope study of tectono-thermal and crustal forming events in the Tomkinson Ranges, western Musgrave Block, Central Australia; 3. Granitic gneiss, Wingellina, Tomkinson Ranges, Western Musgrave Block. Sun, S.S. Gray, C.M. Sheraton, J.W. 1995. Zircon U-Pb chronology and neodymium isotope study of tectono-thermal and crustal forming events in the Tomkinson Ranges, western Musgrave Block, Central Australia|||||3 samples recorded: 1. recrystallised BT gabbronorite (BT-CPX-OPX-PL granulite); 2. foliated BT-HBL granite dyke; 3. ?CPX granite gneiss|
28071|Hinkley Gabbro|70634|5|Briefly described|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic|Sample description: recrystallised BT gabbronorite (BT-CPX-OPX-PL granulite)|1653 Ma - 1693 Ma (Sm-Nd) 1073 Ma (SHRIMP)|||||
34538|Holleton Greenstone Belt|22775|6|Mentioned|2|||||||||
77676|Holmswood Shale|68297|6|Mentioned|p198|||Carnarvon Basin. [misspelling of Holmwood Shale]|||Said to include Fossil Cliff Member.|||
70609|Honman formation|61898|5|Briefly described|p109 Fig. 1|||Informal name.||||||
70609|Honman formation|68108|5|Briefly described|p651 Tb.4|Mesoarchean|Mesoarchean|Southern Cross Domain. U-Pb geochronology by Wang et al. (1996).|ca. 2903 +/- 5 Ma and 2921 +/- 4 Ma||||Felsic volcanic.|
41357|Hooley Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Boolaloo Supersuite.||||||07-FEB-11
41357|Hooley Granite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province.  Of the Boolaloo Supersuite.||||||07-NOV-08
32611|Horse Rocks Granite|46311|14|Not recorded|p.10||Archean|Opposite p.6; map.||||||07-NOV-08
41232|Horseshoe formation|23798|6|Mentioned|p2|||Informal - see Horseshoe Formation. Geological Province: Yilgarn Craton.||||||05-JUL-06
41232|Horseshoe formation|50226|6|Mentioned|p420, p422|||Informal - see Horseshoe Formation.||||||
41232|Horseshoe formation|61848|6|Mentioned|p300, p301|||Informal - see Horseshoe Formation.||||||
38129|Hoya formation|23523|6|Mentioned|p994|||Informal - see Hoya Formation. Of Grant Group.||||||
38807|Hughes dolerite|23931|6|Mentioned|p201 Table 1|||Informal name - see Hughes Dolerite. Geological Province: Yilgarn Craton.||||||
38807|Hughes dolerite|60978|6|Mentioned|p68-69 Fig.3|||Informal reference to a dolerite in the Jundee gold deposit. Geological Province: Yilgarn Craton.||||||25-MAY-05
38807|Hughes dolerite|60979|5|Briefly described|p92, p86 Fig.2, p90|||Part of the Jundee sequence - Jundee goldfield area. Thickness: ~100-150m. See also p91 Fig.4. Fine- to coarse-grained ophitic to sub-ophitic dolerite and quartz granophyre. Medium- to coarse-grained clinopyroxene cumulate at base.||||||27-JUN-05
70753|Hussar Beds''|62453|6|Mentioned|p27|||Superseded by Hussar Formation. ||||||
40108|Hussar beds|24161|6|Mentioned|p11|||Informal - see Hussar Formation.||||||
68828|Hussar beds""|23571|6|Mentioned|p8|||Informal name - upgraded to Hussar Formation (Cockbain and Hocking, 1989). Geological Province: Officer Basin.||||||16-MAY-05
74045|Hyland Bay Sub-group|13222|6|Mentioned|p234.|||Replaced, and later replaced by, the term Hyland Bay Formation.||||||
74045|Hyland Bay Sub-group|13242|4|Described|p214|Late Permian|Early Permian|After Mory (1988, 1991). Of the Kinmore Group. Supersedes Hyland Bay Formation. Geological Province: Bonaparte Basin. Age: Kungurian-Ufimian to latest Permian.||||||21-DEC-12
74045|Hyland Bay Sub-group|64690|5|Briefly described|p503, p504, p505 |Late Permian|Late Permian||||Includes Pearce, Cape Hay, Dombey, Tern and Penguin Formations.|||
74045|Hyland Bay Sub-group|64692|5|Briefly described|p521, p522 Fig.2 |Late Permian|Late Permian|Bonaparte Basin.|||Includes Pearce, Cape Hay, Dombey, Tern and Penguin Formations.|Overlies Fossil Head Formation. Is overlain by Lower Mount Goodwin Formation.||
74045|Hyland Bay Sub-group|67370|5|Briefly described|pp316-318, p332. |Permian|Permian|||Middle unit in Kinmore Group.|Includes Torrens, Pearce, Cape Hay, Dombey and Tern Formations.|Overlies Fossil Head Formation. Is overlain by Mount Goodwin Subgroup.|Contains cool-water limestones.|
74045|Hyland Bay Sub-group|69653|5|Briefly described|p10, 15|Permian|Permian|Petrel Sub-basin.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey, Tern, Penguin Formations.|Overlies Fossil Head Formation. Is overlain by Mount Goodwin Sub-group.||
74045|Hyland Bay Sub-group|70064|5|Briefly described|Regional Fig. 6|Changhsingian|Wordian|Prudhoe Terrace, Browse Basin.||Kinmore Group.||Overlies Kulshill Group. Is overlain by Mount Goodwin Subgroup.||12-JUL-16
74045|Hyland Bay Sub-group|71623|6|Mentioned|p355|||||||Unconformably overlain by Tern Formation.||
41243|Hynds Seam, lower|50603|5|Briefly described|p25|||Informal name.  Average thickness of 8m.||||||
38653|Ida Hill complex|23786|6|Mentioned|p21|||Informal name.||||||
28246|Ilgarari Beds|24183|6|Mentioned|p24|||Superseded by the Ilgarari Formation (Muhling and Brakel, 1985). Of the Bangemall Group.||||||
28246|Ilgarari Beds|29916|5|Briefly described|p120|||||||||
28246|Ilgarari Beds|37460|4|Described|p164|||See also Fig.3.16a.||||||
28246|Ilgarari Beds|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28246|Ilgarari Beds|40899|6|Mentioned|Fig.1|||||||||
28246|Ilgarari Beds|41360|6|Mentioned|Table 1|||||||||
40782|Illaara quartzites|50128|6|Mentioned|p42|||Informally referring to quartzites of the Illaara greenstone belt. Geological Province: Yilgarn Craton.||||||
74844|Illagalara Monzogranite|64891|5|Briefly described|p37 Fig. 2, p52-53 Tb. 1|Archean|Archean|Of the Jungar Suite. Age: c. 2645Ma. Geological province: Murchison Domain. K-feldspar megacrystic monzogranite, occasionally laminated; metamorphosed.||||||07-FEB-11
75772|Illigalara Monzogranite|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Jungar Suite, Yilgarn Craton. 2665-2640 Ma age given for Suite. Metamorphosed pegmatitic granite with feldspar augen.||||||
41202|Imbin rhyodacite|50222|5|Briefly described|p336|Paleoproterozoic|Paleoproterozoic|Informal reference to rhyodacitic subvolcanic rocks of the Imbin Inlier.  Age: 1.99Ga.||||||07-NOV-08
81603|Indee Supersuite|72251|6|Mentioned|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton. Poorly labelled diagram.||||||03-SEP-19
77464|Indoon Member|67370|5|Briefly described|p318 Fig.10, p320. |Early Triassic|Early Triassic|Written as 'Indoon member' in the article: an informal name. Correlated from Indoon-1 to East Lake Logue-1 and into some Woodada gas field wells. Apparently correlated with Ascalon Formation.||Unit in Kockatea Shale.|||Very fine-grained sandstones.|
81347|Indulkana gneiss|70084|5|Briefly described|p226|||Geological province: Musgrave Province, Paterson Orogen. Contains the only occurrence of c. 1700 Ma and older zircons. Isotopically equivalent to Wirku Metamorphics WMb and WMc, but differing in that zircons are of WMc and rimmed by WMb component, and therefore interpreted to be a a high-grade paragneiss that is a partial (anatectic) melt of the Wirku Metamorphics.|~1700 Ma.|||||08-AUG-19
73759|Iowa Eastern Clay|63432|6|Mentioned|p738, p746|||Refers to the clay unit known as Iowa Eastern Member of the Marillana Formation - names are used interchangeably. See also p751.||||||11-APR-16
83268|Iregully Formation|72259|6|Mentioned|App. Tb.B||||||||Includes silicified mudstone.|
81593|Irindina Gneiss, lower''|68997|6|Mentioned|p54|||Nomenclature after Maidment 2005. Informal: see Yambla Gneiss.|||||Garnet-bearing migmatitic metapsammopelite and metapelite, diopside-garnet-bearing calc-silicate rock, marble (mostly impure) and lesser quartzite.|
83147|Irindina Group|72491|5|Briefly described|p61|Cambrian|Cambrian|Arunta Block. Represents a >20 km deep turbiditic rift basin floored by mafic igneous rocks, that experienced fast deposition and peak metamorphism within <10 m.y. of the start of extension.||||||
77109|Iris Marl|60386|6|Mentioned|p302|Kimmeridgian|Kimmeridgian|Browse Basin/Bonaparte Basin. Limestone nearshore-shelf.||||||
77109|Iris Marl|61548|6|Mentioned|p480 Fig.3|Kimmeridgian|Kimmeridgian|Northern Bonaparte Basin.||||||
77109|Iris Marl|68223|6|Mentioned|p178 Fig.3, p180 Fig.5|Kimmeridgian|Kimmeridgian|||||||
28618|Irwin Coal Measures|23279|6|Mentioned|p13|||Miswritten for Irwin River Coal Measures.||||||
28618|Irwin Coal Measures|36266|6|Mentioned|p150|||||||||31-MAR-08
28618|Irwin Coal Measures|43296|6|Mentioned|Map Legend||Permian|||||||
28618|Irwin Coal Measures|44237|14|Not recorded|p.202||Permian|||||||
35918|Irwin River Formation|23356|5|Briefly described|26 Tab.2|Early Permian|Early Permian|||||||
70730|Isdell Formation''|62453|6|Mentioned|p69|||Informal Name. ||||||
78598|Iwuputaka Metamorphic Complex|65487|6|Mentioned|p62|||[Mis-spelling of Iwupataka]. Close et al.,(2006). A sedimentary package deposited c.1630-1610 Ma, ie after the Liebig Orogeny. ||||||
83148|Jack Hills Association|72491|6|Mentioned|p5|Palaeoarchaean|Palaeoarchaean|Narryer Terrane, Yilgarn Craton.||||||
72637|Jack Hills metsediments|62842|6|Mentioned|p217|||Contain zircons with age groups of 3750-3600Ma and 3450-3250Ma.||||||28-NOV-06
72632|Jack Hills quartzite|62842|6|Mentioned|p203|Paleoproterozoic|Paleoproterozoic|White micas age: 1830-1780Ma (Ar-Ar, Spaggiari 2005).||||||07-NOV-08
80087|Jackys Pool Metadolerite Suite|70795|4|Described|100k_geologyl_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_interpgeol_lut.csv|2500-1811 Ma||||Metadolerite, locally with garnet coronas around pyroxene.|
34225|Jaimson Formation|22663|5|Briefly described|AC97 1-4 Fig.4|Late Cretaceous|Early Cretaceous|Bathurst Island Group||||||
40084|Jameison Formation|24207|6|Mentioned|p216|||Misspelt - see Jamieson Formation.||||||
25084|James Range gabbro|38490|6|Mentioned|p308|||||||||
69739|Jameson Range Troctolite|61341|5|Briefly described|Map legend|||Presented in the compound name Jameson Range Troctolite/Gabbro. Intrusion.||||||21-SEP-05
69767|Jameson Range troctolite/gabbro intrusion|44109|4|Described|p10, p88|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Layered Fe-rich troctolite, gabbroic troctolite and anorthosite adcumulates, with various proportions of disseminated magnetite. Thickness: ~2500m.||||||31-JUL-14
69767|Jameson Range troctolite/gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: ~2500m.||||||
77412|Jameson intrusion|65135|5|Briefly described|p14, p16|||Informal name. Broadly troctolitic. Of the Giles intrusions. Probably part of a larger single intrusion including the Blackstone, Finlay and Bell Rock intrusions. Includes xenoliths of Mummawarrawarra Basalt.||||||
77412|Jameson intrusion|65693|5|Briefly described|pp4-5.|||A layered mafic intrusion, cross-cut by gabbro dykes, locally mineralised (Cu, Pd, Pt).|1067 +/-8 Ma SIMS zircon geochronology|||||30-OCT-12
77412|Jameson intrusion|68996|5|Briefly described|p26, 34, 36-41, 47, 50,57,59,61-64,67,68|Mesoproterozoic|Mesoproterozoic|Part of G1 group. ~8km thick. Misspelt as Jamieson intrusion p52.||Giles Suite||Connected at depth with Cavenagh, Blackstone and Bell Rock intrusions.||
28621|Jamieson Formation, Lower|42053|5|Briefly described|Fig.2 p29|||||||||21-OCT-15
28621|Jamieson Formation, Lower|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
28621|Jamieson Formation, Lower|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Informal - see Jamieson Formation. Age: ~114-~106Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||09-NOV-06
28621|Jamieson Formation, Lower|69297|5|Briefly described|p305|Albian|Aptian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Bathurst Island Group||Overlies the Echuca Shoals Formation. Overlain by the Upper Jamieson Formation.|Mudstones or shales.|
28621|Jamieson Formation, Lower|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Browse, Bonaparte Basins.||||Overlies Echuca Shoals Formation.||
28621|Jamieson Formation, Lower|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Albian|Aptian|See also Northern: Fig.2; p1. Yampi: Fig.2. Browse Basin. Oil-prone, immature-marginally mature shallow marine source rocks. Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoir.||Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Upper Jamieson Formation.|Includes shallow-marine sandstones, submarine fans and ponded turbidites.|12-JUL-16
69621|Jamison Sandstone|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
69621|Jamison Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
69621|Jamison Sandstone|62759|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Geological Province: Beetaloo Sub-basin.  Contains oil reservoirs.||||||05-FEB-08
69621|Jamison Sandstone|64784|4|Described|p2-10     |Proterozoic|Proterozoic|Beetaloo Basin. A key reservoir in the Basin. Widespread; thickness from 100 to 160 m. Organics content from 2% to 6%.||Unit in Roper Group.||Unconformably overlies the Kyalla Formation. Conformably (transitionally) underlies the Hayfield Mudstone.|Approximately 100m thick. Light to medium-gray sandstone, very fine- to medium-grained, and moderately to well sorted. Generally coarsens upwards.|24-JUN-14
69621|Jamison Sandstone|64975|6|Mentioned|p162 Fig.6.|Neoproterozoic|Neoproterozoic|||||||
69621|Jamison Sandstone|65236|6|Mentioned|p1, p2, p3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Overlies the Kyalla Formation. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
69621|Jamison Sandstone|69018|5|Briefly described|p450 Fig.1b, p451|||Oil from Jamison-1 well discussed & compared with Bessie Creek Sandstone oil. ||Of Roper Group.|Unconformably overlies Kyalla Formation & thus also younger than Velkerri Formation, Bessie Creek Sandstone.|||
69621|Jamison Sandstone|70968|5|Briefly described|p86|||Subsurface Beetaloo Sub-basin. Lanigan et al. (1994), for two sandstone-rich units unconformably overlying Kyalla Formation and underlying their Hayfield Mudstone. Subsequently Jamison sandstone (?Gorter and Grey, 2012): see references (v-vi, p75, p77, p81, p86-90, p124-129).||||||
69621|Jamison Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||||Overlies Bukalorkmi Sandstone, Roper Group and underlies Hayfield Mudstone.||
69621|Jamison Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||||Underlain by Bukalorkmi Sandstone. Overlain by Hayfield Mudstone.||
70617|Jandakot sediments|62369|6|Mentioned|p414|||Informal - see Jandakot Member.||||||
25085|Jap Bay Formation|39948|6|Mentioned|Fig.2|||||||||
82942|Jarrad Member|73255|4|Described|p532, p538-539, p543-544, p546, p548-549|Ediacaran|Ediacaran|Dolomitic sandstones contain dessication cracks and mineral weathering trends of dolomite depletion, identified as paleosols. Fluvial paleochannel facies of dolomitic sandstone are capped by paleosols and eolian siltstones, best developed soil type of the unit interpreted as orthic solonchak. Mean annual precipitation estimated to be 265-325 mm based on paleosols, mean annual range of precipitation of 37-48 mm and cool to frigid tempreatures. Specific locations in text include p538 Fig.5, p539 Fig.6, p541. [Recorded in database as Jarrad Sandstone Member?]||Ranford Formation||Conformably overlies the Moonlight Valley Tillite, underlies the Johnny Cake Member.|Dolomitic sandstones with calcareous nodules, thick sandstone beds are capped by thin interflag sandstone laminae of fine-grained sandstone and siltstone.|
73580|Jean Granodiorite|63441|6|Mentioned|p37|Archean|Archean|Probably misspelt - see Jean Well Granodiorite.||||||07-FEB-11
31098|Jeedamya Rhyodacite|43478|2|Defined|p13-61|||||||||
78968|Jeedamya Rhyolite|63980|5|Briefly described|p64 Table 2|Archean|Archean|Of the Gindalbie Sequence [~Gindalbie Terrane?]. See also Jeedmya Complex pp73, 63.|2681 +/- 5 Ma U/Pb SHRIMP (Nelson 1997b)||||Porphyritic rhyolite and rhyodacite, felsic volcanogenic sandstone and breccia, basalt, dolerite.|26-SEP-14
78968|Jeedamya Rhyolite|67198|6|Mentioned|p69|Neoarchean|Neoarchean|Ages from felsic volcanic rocks of the Rifle Range and Teutonic Bore localities respectively.|2680 +/- 2 Ma, 2694 +/- 4 Ma|||||11-SEP-17
77550|Jeedamya Rhyolite Complex|66880|6|Mentioned|p9, p27. |Archean|Archean|Very similar age to rhyolite from Melita Complex to the north. Geochemically similar to calc-alkalic volcanic and volcaniclastic Kurnalpi Sequence rocks, reflecting similar intra-arc or arc-related basins.|2681 +/- 5 Ma (Nelson 1997).|||||01-NOV-12
40769|Jeedamya complex|24196|6|Mentioned|p8, p42|||Informal - see Jeedamya Complex.||||||
40769|Jeedamya complex|24494|6|Mentioned|p23 Tb.2|||Informal - see Jeedamya Complex.||||||
41111|Jeedamya rhyolite complex|24196|5|Briefly described|p44|Archean|Archean|Informal - see Jeedamya Complex. Age: 2681 +/- 4 Ma.||||||07-NOV-08
40770|Jeedamya volcanic complex|24494|6|Mentioned|p22|||Informal - see Jeedamya Complex.||||||
40770|Jeedamya volcanic complex|69631|5|Briefly described|p48|Neoarchean|Neoarchean|Melita area. Likely that this will be assigned to the Melita Formation.|c.2681 Ma (Nelson, 1996).||||Dacite and rhyolite pyroclastic rocks and related epiclastic rocks, felsic porphyry, and minor mafic extrusive and intrusive rocks.|
70205|Jeerinah Formation, upper|61575|5|Briefly described|p760, p763, p766|||Informal - see Jeerinah Formation.  Contains the Jeerinah spherule layer. ||||||
79180|Jeerinah Shale|65757|5|Briefly described|p85|||Of Simonson, 2000. Underlies the Marra Mamba Iron Formation. See also Jeerinah Formation p81 Tb.2.||||||
70206|Jeerinah impact layer|61575|5|Briefly described|p766|||Informal - see Jeerinah Formation.  Refers to the Jeerinah spherule layer. ||||||
70206|Jeerinah impact layer|70733|5|Briefly described|p108, 117-118, 120|||Appears mysteriously as JIL on p108, then 117 and 120. Comparison of PGE values with those in Marble Bar Chert Member.|2629+/-5 Ma (Glikson and Hickman, 2014)|Fortescue Group.||Overlies Roy Hill Member.|Spherule-rich units containing brown argillite intraclasts.|
70183|Jeerinah layer|61560|5|Briefly described|p498 Tb. 4|||Informal reference to Jeerinah Formation.||||||
70207|Jeerinah spherule layer|61575|3|Fully described|p760, p763-764|Neoarchean|Neoarchean|Informal - refers to spherule layer within the Jeerinah Formation; interpreted as impact-generated melt. Geological Province: Hamersley Basin.||||||07-NOV-08
70207|Jeerinah spherule layer|61576|5|Briefly described|p774 Fig. 1|Neoarchean|Neoarchean|Informal name - refers to impact spherule layer within the Jeerinah Formation. Age: 2629+/-5Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
73595|Jeerinah stromatolite|62579|6|Mentioned|p116|Archean|Archean|Informal reference to the stromatolite occurrences in the Jeerinah Formation. Geological Province: Pilbara Craton||||||07-NOV-08
31847|Jerramungup Adamellite|45003|6|Mentioned|p79|||See also Lexicon||||||
42428|Jiliyili Formation|24535|5|Briefly described|p2|||Of Salvation Group. Previously included in Kahrban Subgroup and previously correlated with Sunbeam Group. [Misspelt - see Jilyili Formation p4 Fig. 2].||||||26-NOV-13
40746|Jillawarra Formation""|24183|6|Mentioned|p1|Mesoproterozoic|Mesoproterozoic|The use of this term has been abandoned - now obsolete.||||||
79776|Jillyili Formation|64625|6|Mentioned|p258|||Savory Sub-basin (Western Officer Basin). Contains mafic sills of similar composition and age to those in the Bitter Springs Formation (Amadeus Basin).||||||
68977|Jimba Jimba|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Informal. Geological Province: Carnarvon Basin||||||
32764|Jimba Jimba Formation|45016|14|Not recorded|p.92|||||||||
36144|Jimberlana Complex|23449|6|Mentioned|p524|||||||||
29757|Jimperding Complex|43030|5|Briefly described|Map Legend|||||||||
29757|Jimperding Complex|43038|6|Mentioned|p8|||||||||
29757|Jimperding Complex|43189|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
29757|Jimperding Complex|43212|5|Briefly described|p1,p2.||Archean|||||||07-NOV-08
37188|Joffre formation|23612|6|Mentioned|p846|||Misspelt - see Joffre Member||||||
82941|Johnny Cake Member|73255|4|Described|p532, p537, p539, p541, p543-544, p548|Ediacaran|Ediacaran|Interbedded red-green siltstone facies includes gypsum rosettes, desiccation cracks, claystone breccias, planar and wavy bedding, Rugalichnus and Rivularites trace fossils. interpreted depositional environment of a shallow lacustrine basin, comparable with dry lake gypsids or solonchak soils. Some thin siltstone layers show inverse grading, characteristic of climbing translatent bedding formed by wind. Main components of zebra rock are kaolinite, quartz and dickite, minor sericite, alunite, ferrihydrite; may have weathered from tuffs deposited in poorly drained basins with acid sulfate weathering, seasonally waterlogged and redoximorphic soil in an arid climate. Specific locations in text include p537 Fig.4, p539 Fig.6. [Recorded in database as Johnny Cake Shale Member?]||Ranford Formation||Overlies the Jarrad Member.|Contains discontinuous lenses of zebra rock comprising intensely weathered clayey siltstone beds with red and grey bands, enclosed in laminated to varved shales, interbedded red and green siltstone, shales and thin sandstones.|
78779|Johnny Cake Sandstone Member|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|Presented as Johnny Cake Sst M in figure.||Unit in Ranford Formation.||||
23673|Johnson Cairn Shale|7161|5|Briefly described|p92,  p92 Fig.4, p94, 100|||Neds Creek Basin. Submarine-fan Floodbasin. Approximately 1000m thick (from p92 Fig.4).||||Laterally equivalent to the Thaduna Greywacke. Underlain by the Narracoota Volcanics.|Quartzose sandstone and lithofacies typical of shoreface, barrier-bar and tidal-platform systems, overlain by mudrock and pyritic organic-rich shale of an interpreted offshore restricted-marine or lacustrine system.|02-MAY-12
23673|Johnson Cairn Shale|12099|6|Mentioned|p678 Fig.4|||Superseded by Johnson Cairn Formation. Placed in Glengarry Group by Gee (1987) and Gee and Grey (1993)||||||
23673|Johnson Cairn Shale|22493|5|Briefly described|p94|||||||||
23673|Johnson Cairn Shale|23600|6|Mentioned|p8|||Renamed Johnson Cairn Formation.||||||
23673|Johnson Cairn Shale|23749|6|Mentioned|p7|||Superseded by Johnson Cairn Formation.||||||
23673|Johnson Cairn Shale|40297|6|Mentioned|Fig.1|||||||||
23673|Johnson Cairn Shale|40938|6|Mentioned|p10|||Mention Fig.5||||||
23673|Johnson Cairn Shale|40989|4|Described|p16|||||||||
23673|Johnson Cairn Shale|42260|6|Mentioned|p125|||||||||
23673|Johnson Cairn Shale|43069|1|Redefined|p30|Mesoproterozoic|Paleoproterozoic|refer to Gee (1987) for original definition.||||||07-NOV-08
23673|Johnson Cairn Shale|49893|6|Mentioned|p13|Proterozoic|Proterozoic|Superseded by the Johnson Cairn Formation.||||||
23673|Johnson Cairn Shale|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1987, 1990).||||||
23673|Johnson Cairn Shale|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Of former Glengarry Group. Gee (1987) and Gee and Grey (1993); superseded by Johnson Cairn Formation (Occhipinti et al. 1997)||||||
23673|Johnson Cairn Shale|64384|5|Briefly described|p78 Tb. 8|||Of the Glengarry Group. Overlies Juderina Formation. Geological province: Glengarry Sub-basin. Shale.||||||07-FEB-11
23673|Johnson Cairn Shale|65419|6|Mentioned|p17.|Paleoproterozoic|Paleoproterozoic|Of Gee (1987) and Gee and Grey (1993). Strata now included in Johnson Cairn Formation; name changed to reflect the heterolithic nature of the strata.||||||
23673|Johnson Cairn Shale|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. 150-250m thick sandstone-chert-shale epeiric-sea facies.||Glengarry Group||||
23673|Johnson Cairn Shale|70804|5|Briefly described|p2|||Obsolete name, replaced by the Johnson Cairn Formation of the Windplain Subgroup.||Glengarry Group||||
78816|Johnson Formation Dolomite|64689|6|Mentioned|p13 Fig.13|Paleocene||[unintentional capitalisation of dolomite lithology?]||||||18-MAR-14
72630|Johnson/Basset Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Paleocene|Informal compound name to include both Johnson and Basset Formations. Age: 65-~56Ma. Geological Province: Londonderry High.||||||
81588|Jones Creek Formation|72057|5|Briefly described|p244|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. See also Jones Creek Group p238.|||Includes Scotty Creek Sandstone.|||03-SEP-19
81588|Jones Creek Formation|73391|6|Mentioned|p22||||||||Interpreted as typical molasse depositional system of fluvio-deltaic and fluvio-lacustrine fault-bound basin deposits.|
81588|Jones Creek Formation|73596|6|Mentioned|p1152, 1154-1155, 1158-1161|Neoarchean|Neoarchean|Aouker and Whelan (1990). Agnew-Wiluna Greenstone Belt. Alluvial fans and braided river system at foot of orogenically uplifted mountain belts?|2662 +/- 5 Ma (MDA).|||Unconformably overlies Kathleen Valley Layered Intrusive Complex.||
81584|Jones Creek Group|72057|6|Mentioned|p238|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. See aslo Jones Creek Formation p244.||||Shown as roughly equivalent to Merougil Group.||03-SEP-19
28627|Jones Creek Pegmatite|35113|6|Mentioned|p35|||||||||
28627|Jones Creek Pegmatite|37795|6|Mentioned|Table 4|||||||||
77551|Jones Creek Sequence|66880|6|Mentioned|p8. |Archean|Archean|There is a formally-named unit, the Jones Creek Conglomerate. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank.||||||
77555|Jones Creek Supersequence|66936|5|Briefly described|p137, pp144-147.|Archean|Archean|Northern Kalgoorlie Terrane. Interpreted to be time-equivalent of Kurrawang Supersequence. Thickness to 1050 m. Deposits of proximal braided rivers and within-channel sheet bars.|||||Clast-supported, massive cobble-boulder conglomerate; plane-bedded coarse-grained quartzofeldspathic sandstone; minor medium-grained channel-fill sandstone, and massive, very coarse-grained pebbly quartzofeldspathic sandstone.|
77555|Jones Creek Supersequence|66938|6|Mentioned|pp187-188. |Archean|Archean|An axial (fluvial environment) system, with transport to the south or southeast, implying north to south paleoslopes. Depositional facies are characterisitic of high-discharge bedload draining areas of high relief.|Detrital zircons 2665 +/- 5 Ma.|||||
41112|Jones Creek conglomerate|24196|6|Mentioned|p40, p62|||Informal - see Jones Creek Conglomerate.||||||
32765|Joolabroo Formation|44344|14|Not recorded|p.19, opp.4,map|||(G50-1).||||||
32765|Joolabroo Formation|44345|14|Not recorded|map legend||Pleistocene|||||||
32765|Joolabroo Formation|44532|4|Described|p.11, map|||(G50-5).||||||
32765|Joolabroo Formation|44533|5|Briefly described|map legend||Pleistocene|Pleistocene.||||||
32765|Joolabroo Formation|44537|14|Not recorded|map legend||Pleistocene|||||||
32765|Joolabroo Formation|44657|14|Not recorded|p.5,6,14|||||||||
32765|Joolabroo Formation|45016|14|Not recorded|p.138,163||Quaternary|||||||
32765|Joolabroo Formation|48610|14|Not recorded|Pl.1|||||||||
32765|Joolabroo Formation|48823|6|Mentioned|p30|||||||||
39253|Jubilee Calcarenite Member|24094|5|Briefly described|p276|||Name used interchangably with Jubilee Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
25094|Jubilee Calcarenite""|41271|6|Mentioned|p166|||||||||
35667|Jubilee Dolerite|23140|4|Described|p221|||||||||
37103|Juderina Formation""|23749|6|Mentioned|p6|||See Juderina Formation.||||||
24323|Juderina Sandstone|35975|2|Defined|p100|Proterozoic|Proterozoic|||||||
24323|Juderina Sandstone|38994|6|Mentioned|Fig.1|||||||||
24323|Juderina Sandstone|40297|6|Mentioned|p109|||||||||
24323|Juderina Sandstone|40938|6|Mentioned|p10|||See also P69||||||
24323|Juderina Sandstone|43069|6|Mentioned|p29|||Superseded by Juderina Formation||||||
24323|Juderina Sandstone|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Superseded by Juderina Formation. ||||||
24323|Juderina Sandstone|65419|6|Mentioned|p8, p12.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979). Type area is 3.5 km north of Juderina Bore.||||||
30021|Juglah Granite|43075|6|Mentioned|p13|||Misspelling/variation on Juglah Monzogranite?||||||
82943|Julie Limestone|73255|6|Mentioned|p532|Ediacaran|Ediacaran|Contains the stromatolite Tungussia julia.|||||Limestone.|
38974|Julie formation|23806|6|Mentioned|p1131|||Informal - see Julie Formation.||||||
41084|Junction dolerite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain.  Age: 2681 +/- 5Ma (zircon). Of the Black Flag Beds.||||||07-NOV-08
35676|Jundee Dolerite|23149|5|Briefly described|p101 Fig.5|||||||||
77552|Jundee Mine Sequence|66880|5|Briefly described|p9, p13. |Archean|Archean|Has some relationship with the Middle Greenstone Sequence of Yandal Belt.|2673 +/- 5 Ma.||||Includes dacite pumice breccia.|
40445|June Hill Volcanics, lower|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt. Of the Wyloo Group. See also p861 Fig.4. Informal - see the June Hill Volcanics.||||||
40444|June Hill Volcanics, upper|24602|5|Briefly described|p854 Fig. 1|||Geological Province: Ashburton Fold Belt. Of the Wyloo Group. See also p861 Fig.4. Informal - see the June Hill Volcanics.||||||
41233|June Hill volcanics|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Informal name.  At base of the Ashburton Formation of the upper part of the Wyloo Group.  Age: 1.84 Ga (Pidgeon and Horwitz, 1991).||||||07-NOV-08
41233|June Hill volcanics|69745|6|Mentioned|p270-271|||Hamersley Province. Formed during a rifting event associated with development of the Ashburton Trough. Presented as June Hill volcanic sequence.|c.1800 Ma.|||Overlies the Mount McGrath Formation.|Bimodal volcanic sequence.|
34387|June Hill-Mount Boggola Supersequence|22682|5|Briefly described|Fig21,p31|Orosirian|Orosirian|1862-1815 Ma. Ashburton Province||||||03-MAR-10
40771|Jungle monzogranite|24494|6|Mentioned|p21|||Informal - see Jungle Monzogranite||||||
25966|Jurgurra Sandstone|32648|6|Mentioned|p32|||U. Jur.||||||
25966|Jurgurra Sandstone|33166|6|Mentioned|p67|||Stratigraphy||||||
25966|Jurgurra Sandstone|36890|3|Fully described|p347|||||||||
25966|Jurgurra Sandstone|44040|14|Not recorded|p43|||||||||
25966|Jurgurra Sandstone|44998|2|Defined|p130||Jurassic|Underlies Alexander Formation. Probably equivalent to base of Callawa Formation. On many pages. p.119,131-5,148,184, map.||||||
25966|Jurgurra Sandstone|45153|2|Defined|App.6-110|Middle Jurassic|Middle Jurassic|||||||
25966|Jurgurra Sandstone|46860|4|Described|p314|||Re facies.||||||
25966|Jurgurra Sandstone|48837|14|Not recorded|p.6,13|||||||||
32774|Just-in-Time conglomerate beds|45923|14|Not recorded|p148|||||||||
81333|K-M Volcanics|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton. [Likely to be referring to Kantie-Murdana Volcanics Member].|||Unit of Yaloginda Formation.|||
34953|Kahrban Group|22896|6|Mentioned|103|||Geol province Officer Basin||||||
34953|Kahrban Group|62453|6|Mentioned|p52|||Previously included Coonabildie Formation.||||||
34953|Kahrban Group|66107|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Eastern Capricorn Orogen.||||Possible correlative of Collier Group.||
23677|Kahrban Subgroup|22589|6|Mentioned|p125||Proterozoic|||||||
23677|Kahrban Subgroup|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
23677|Kahrban Subgroup|23156|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|The Kahrban Subgroup occupies the Southeastern corner of BULLEN.||||||
23677|Kahrban Subgroup|23749|5|Briefly described|p15|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
23677|Kahrban Subgroup|24017|5|Briefly described|p21|||Of the Bangemall Group.||||||07-AUG-08
23677|Kahrban Subgroup|24183|5|Briefly described|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin. Of the Bangemall Group.||||||
23677|Kahrban Subgroup|40089|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|||||||
23677|Kahrban Subgroup|40938|6|Mentioned|Fig.3|||||||||
23677|Kahrban Subgroup|42708|5|Briefly described|Plate 1|Proterozoic||||||||
23677|Kahrban Subgroup|43209|5|Briefly described|map legend||Mesoproterozoic|of Bangemall Group.||||||
23677|Kahrban Subgroup|43229|5|Briefly described|Map Legend||Mesoproterozoic|of Bangemall Group||||||
23677|Kahrban Subgroup|43492|6|Mentioned|9||Proterozoic|||||||
23677|Kahrban Subgroup|43595|6|Mentioned|Fig 3-43,p348|||Age: 1.0-1.1 Ga||||||
23677|Kahrban Subgroup|43756|6|Mentioned|Fig.1,p534|||||||||
23677|Kahrban Subgroup|44142|5|Briefly described|p309 Fig.4-13, p310 Tb.4-3, p311|||See also p315 Tb.4-4, p321, p324. SE corner of Bangemall Basin.||Bangemall Group|Includes Marlooyanoo and Coonabildie Formations.|Unconformably overlies Scorpion Subgroup. Correlative of Collier Subgroup.||
23677|Kahrban Subgroup|50188|5|Briefly described|p15-16|||Name abandoned. Formerly of the Bangemall Group. Included Cornelia, Coonabildie and Marlooyanoo Formations until mapping indicated that Marlooyanoo Formation is indistinguishable from Coonabildie Formation.Geological Province:  Officer Basin.||||||16-JUL-08
38133|Kahrban Subgroup ""|23529|5|Briefly described|p7|||Geological Province: Bangemall Basin||||||
38133|Kahrban Subgroup ""|50188|6|Mentioned|p9, 16|||Informal. See Kharban Subgroup. Name abandoned. Previously of the "Wandiwarra Formation", and Windidda Formation.||||||16-JUL-08
23678|Kalbarri Group|1943|5|Briefly described|p373, p376|||Of Hocking (1985). Previously defined containing units now known to be of Cambrian to Devonian age, major hiatuses and erosional episodes. This paper proposes term be dropped.||||||
23678|Kalbarri Group|6943|6|Mentioned|p599.|||Pre-Givetian part of Carnarvon Basin.|||Two sandstone-carbonate couplets: Tumblagooda Sandstone-Dirk Hartog Formation, and Kopke Sandstone-Sweeney Mia Formation.|||
23678|Kalbarri Group|22814|5|Briefly described|fig2|||||||||
23678|Kalbarri Group|40617|2|Defined|p1|Silurian|Silurian|||||||
23678|Kalbarri Group|40992|6|Mentioned|Fig.8|||||||||
23678|Kalbarri Group|41271|4|Described|p27|||||||||
23678|Kalbarri Group|42030|6|Mentioned|Fig.2 P744|||||||||
23678|Kalbarri Group|42116|4|Described|p9|||See also Fig.1||||||
23678|Kalbarri Group|42441|4|Described|p3|||||||||
23678|Kalbarri Group|42442|6|Mentioned|p6|||Carnarvon Basin||||||
23678|Kalbarri Group|67200|6|Mentioned|p18 table 1, p51||||||Includes Kopke Sandstone, Sweeney Mia Formation, Dirk Hartog Formation|||
77091|Kalgoorlie Sequence|63981|5|Briefly described|p91, p93 Fig.3, |Archean|Archean|In this study, a section of the Black Flag Group, with characteristic conglomerate-rich facies. One of four unconformity-bounded second-order sequences recognised in the Kalgoorlie Terrane. There is a formally-named unit, the Kalgoorlie Group.|||||Conglomerate, rhyolite, dacite, andesite and basalt; overlapped intrusions of gabbro and I-type granitoids; deformed and metamorphosed to lower greenschist facies.|
77091|Kalgoorlie Sequence|64633|5|Briefly described|p4 Fig.3. |||Kalgoorlie Terrane.|c.2692 - c.2665 Ma.||Includes Black Flag, White Flag, and Spargoville Formations.|Overlies Kambalda Sequence.||
77091|Kalgoorlie Sequence|66880|4|Described|p7, pp25-28, p30.|Archean|Archean|Middle of three lithostratigraphic divisions in the Kambalda Domain. TTD felsic volcanism and associated volcaniclastic and epiclastic sedimentation between 2687-2676 Ma and again between 2669-2665 Ma.|2686 +/- 3 Ma to 2658 +/- 3 Ma.|||Intruded by Mount Shea and Kanowna Belle porphyries.|Felsic volcaniclastic rocks.|
77091|Kalgoorlie Sequence|66936|6|Mentioned|pp136-137. |Archean|Archean|Kalgoorlie Terrane.||||Is unconformably overlain by Kurrawang and Merougil Supersequences.||
77091|Kalgoorlie Sequence|66938|5|Briefly described|p186. |Archean|Archean|Kalgoorlie Terrane. Contains intra-arc basins that are unconformably overlain by Kurrawang and Merougil Supersequences. 32 My of successive intra-arc basins culminated at c.2685 Ma in WSW-directed recumbent folding and thrust faulting.|||||Includes felsic volcanic rocks of TTG affinity and mafic rocks of tholeiitic composition.|
77091|Kalgoorlie Sequence|67198|4|Described|p5 Fig.2, p7, p16, p69, p81-83, p89,p112|Neoarchean|Neoarchean|Kalgoorlie Terrane. See also p114, p118, p122, p136.|Between 2686 +/- 3 Ma and 2658 +/- 3 Ma.||Black Flag Group, White Flag Formation, Spargoville Formation|Unconformably overlies the Kambalda Sequence. Is overlain unconformably by Kurrawang Sequence.|Andesite, dacite, rhyolite volcaniclastic and epiclastic rocks, minor lavas and sedimentary siliciclastic rocks, local felsic volcanic centres, and dolerite sills.|11-SEP-17
77091|Kalgoorlie Sequence|68107|6|Mentioned|p618, p619 Fig.8, p621|Neoarchean|Neoarchean|Kalgoorlie Terrane.|ca. 2686-2666 Ma||||Felsic volcanic and volcaniclastic rocks.|
77091|Kalgoorlie Sequence|68108|6|Mentioned|p652|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane.|ca. 2686 - >2658 Ma||||Concurrent volcanic-granite magmatism.|08-OCT-14
77091|Kalgoorlie Sequence|68109|5|Briefly described|p660|Neoarchean|Mesoarchean||2690 - >2658 Ma|||Equivalent to Black Flag Group. Unconformably overlain by the Merougil and/or Kurrawang Sequence.|Felsic volcanics and volcaniclastics.|
77091|Kalgoorlie Sequence|68186|5|Briefly described|p5|Archean|Archean|Kalgoorlie Terrane, Eastern Goldfields Superterrane.|2686-2666 Ma.|||Overlies Kambalda Sequence.|Felsic volcanic and volcaniclastic rocks.|
77091|Kalgoorlie Sequence|68289|5|Briefly described|p6|||Kalgoorlie Terrane. Of Krapez and Hand (2008). Interpreted as representing a strike-slip intra-arc basin.||||||
77091|Kalgoorlie Sequence|69091|5|Briefly described|p31|||Of Kalgoorlie Terrane in western part of Eastern Goldfields Superterrane.|c. 2686-2666 Ma e.g. Kositcin et al. (2008)||||Felsic.|
77091|Kalgoorlie Sequence|69404|6|Mentioned|p4, p4 Fig.4|Neoarchean|Neoarchean|Kalgoorlie Terrane.||||Overlies the Kambalda Sequence.|Conglomerate with felsic volcanic and volcaniclastic rocks.|
77091|Kalgoorlie Sequence|69583|6|Mentioned|p35|||Krapez and Hand (2008); equivalent to the Black Flag Group.||||||
77091|Kalgoorlie Sequence|69586|5|Briefly described|p1||||2686-2666 Ma.|||Overlies the Kambalda Sequence.|Felsic volcanic and volcaniclastic rocks.|
77091|Kalgoorlie Sequence|69619|5|Briefly described|p115|Neoarchean|Neoarchean|Deposited in two tectonic stages: SHRIMP U-Pb zircon ages by Krapez et al. (2000), Czarnota et al. (2010) and Squire et al. (2010).|2681-2670 Ma and 2661-2655 Ma.|||Is intruded by Golden Mile Dolerite.|Volcanic rocks of rhyolitic to andesitic composition, quartzo-feldspathic siltstones, oligomictic and polymictic conglomerates.|
77091|Kalgoorlie Sequence|69631|6|Mentioned|p6, p26|||Krapez and Hand (2008); apparently their term for rocks of the Black Flag Group. Interpreted as representing a strike-slip intra-arc basin.||||||
77091|Kalgoorlie Sequence|70020|4|Described|p117,121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Thickness: >3km. |2690-2660 Ma||Includes Black Flag Formation. White Flag Formation and Spargoville Formation.||Volcaniclastic rocks, felsic volcanic rocks, mafic intrusive complexes with minor mafic volcanic rocks.|
77091|Kalgoorlie Sequence|70276|6|Mentioned|p783|||Kalgoorlie terrane, Yilgarn Craton.||Black Flag Group.|||Part of a complex felsic volcaniclastic succession.|
77091|Kalgoorlie Sequence|70287|5|Briefly described|p188, 190, 192, 210|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton. This minimum depositional age (Krapez et al., 2000) is from a cross-cutting porphyry dyke.|2658 +/- 3 Ma (minimum).||Black Flag Beds.|Unconformably overlies Paringa and Devon Consols Basalts.||
77091|Kalgoorlie Sequence|70326|5|Briefly described|p337|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Dominated by ~2690-2670 Ma deep-marine siliciclastic and volcaniclastic sediments, unconformably ove-lain by ~2670-2655 Ma subaerial volcaniclastic and siliclastic sediments (Barley et al., 2008; Krapez et al., 2008; Krapez and Hand, 2008; Squire et al., 2010).|~2690-2655 Ma|||Underlain conformably by Kambalda Sequence.||
77091|Kalgoorlie Sequence|70482|6|Mentioned|p317-319, 321, 323, 325, 329|Archean|Archean|Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Intra-arc to backarc environment. Deformations described. Hosts the Gordon-Sirdar Au mine.||||Overlies the Kambalda Sequence. Is overlain unconformably by Panglo sandstone.|Coarse volcanic and sedimentary units, including sheared felsic and mafic-intermediate conglomerate and fragmental rocks.|
77091|Kalgoorlie Sequence|70773|5|Briefly described|p18 fig 11|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane.|||Includes the Spargoville Formation, White Flag Formation and the Black Flag Formation.|||
77091|Kalgoorlie Sequence|71148|5|Briefly described|p121-122|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Over 3km thick.|2690-2660 Ma.|||Overlies Kambalda Sequence.|Package of (mainly turbiditic) volcaniclastic rocks, felsic to intermediate rocks, and mafic intrusive complexes with minor mafic volcanic rocks.|
77091|Kalgoorlie Sequence|71168|5|Briefly described|p8-p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton. More than 3km thick.|c. 2690-2660 Ma|||Overlies the Kambalda Sequence.|Volcaniclastic rocks, felsic volcanic rocks and minor mafic volcanic rocks.|
77091|Kalgoorlie Sequence|71308|6|Mentioned|p711 Fig.2|||Kalgoorlie Terrane.||||||
77091|Kalgoorlie Sequence|71309|6|Mentioned|p740 Fig.3|||||||||
77091|Kalgoorlie Sequence|72049|5|Briefly described|p255-p258, p268|||This name is used for the thick packages of predominantly felsic clastic rocks that overlie the Kambalda Sequence.||||Overlies the Kambalda Sequence.||
77091|Kalgoorlie Sequence|72057|5|Briefly described|p237-238,242|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. Commonly referred to as Black Flag Group. Divisible into early and late successions based of provenance and U-Pb detrital-zircon characteristics (Squire et al., 2010). Coeval with voluminous felsic plutonism.|c. 2690-2660 Ma|||Overlain conformably to unconformably  by Kalgoorlie Sequence/Black Flag Group.||
77091|Kalgoorlie Sequence|72485|5|Briefly described|p3 Fig.2||||2690-2660 Ma.||Black Flag Formation, White Flag Formation, Spargoville Formation.|Overlies the Kambalda Sequence.||
77091|Kalgoorlie Sequence|73151|6|Mentioned|p15|||Yilgarn Craton. Has intrusive contacts with regionally extensive granitoid plutonism between 2700 Ma and 2665 Ma in the Eastern Goldfields Superterrane.||||||
77091|Kalgoorlie Sequence|73238|5|Briefly described|p6, 18|||Leonora district.|c.2720-2660 Ma.|||Is overlain unconformably by Kurrawang and Merougil Formations.|Includes rhyolite.|
77091|Kalgoorlie Sequence|73300|6|Mentioned|p1112-1113|||Yilgarn Craton, Kalgoorlie terrane.|||Black Flag Group|Overlies the Kambalda Sequence.||
77091|Kalgoorlie Sequence|73391|5|Briefly described|p208, 217, 221, 235, 435, Appendices.|||Krapez et al. (2000), to comprise Spargoville Formation, Black Flag Formation and White Flag Formation, each separated unconformably.|||||Coarse-grained andesitic epiclastic turbidites, olistoliths of pillowed and massive andesite.|
25099|Kalgoorlie greenstones|23924|6|Mentioned|p211 Fig. 4|||Geological Province: Yilgarn Craton.||||||
25099|Kalgoorlie greenstones|24494|6|Mentioned|p12|||Informal name.||||||
25099|Kalgoorlie greenstones|31038|6|Mentioned|Fig. 2|||Archaean||||||
25099|Kalgoorlie greenstones|31039|6|Mentioned|Fig. 2|||||||||
25099|Kalgoorlie greenstones|60076|4|Described|p11, p16 Fig. 6|Archean|Archean|An informally named sequence of rocks consisting of a lower basalt unit overlain by a komatiite unit followed by felsic volcanic and sedimentary rocks.  Comprises the Ginbaldie, Bullabulling and Ora Banda domains grouped together.||||||07-NOV-08
77092|Kalgoorlie sequence|64633|5|Briefly described|p8. |||Kalgoorlie Terrane. Part of a greenstone succession; deposited in an extensional, deep-marine, ?intra-arc basin.|||Includes Black Flag Group.||A tonalite-trondhjemite-granodiorite volcaniclastic association.|
77092|Kalgoorlie sequence|70087|6|Mentioned|p215|Archean|Archean||>2680 Ma.|||||
41435|Kaliranu Beds|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
37152|Kaliranu beds|23758|5|Briefly described|p10|||Informal - Replaced by Kaliranu Member. Geological Province: Yeneena Basin.||||||
37152|Kaliranu beds|44139|5|Briefly described|p278 Table 3-13, p279 Table 3-14, p282|Neoproterozoic|Neoproterozoic|>350m. Poorly outcropping silty dolomite, shale, sandstone. Northeastern zone of Yeneena Basin. Conformably overlies Wilki Quartzite. See also mis-spelt Kalirunu beds p280.| | ||||05-MAR-18
70731|Kaliranu beds''|62453|6|Mentioned|p69|||superseded by Kaliranu Member||||||
77184|Kalirunu beds|44139|5|Briefly described|p280|||Conformably overlies Wilki Quartzite. Mis-spelling of Kaliranu beds (see p278-279).| | ||||05-MAR-18
81165|Kalkarindji Basalt|70315|6|Mentioned|Fig 3 p24|||Kalkarindji Province.||||||12-JUN-19
80058|Kalkarindji Supersuite|69634|4|Described|GEOL_LUT_CSV files|||Of Kalkarindji Large Igneous Province. Events: Alice Springs Orogeny. See 250k_interpgeol_lut.csv, 250k_geologyl_lut.csv.|||Includes Milliwindi Dolerite.|||
80058|Kalkarindji Supersuite|70154|6|Mentioned|100k_geologyp_lut.csv|Cambrian|Cambrian|See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv.|||Milliwindi Dolerite|||
80058|Kalkarindji Supersuite|70826|6|Mentioned|p14 tbl 5|Cambrian|Cambrian|NW Officer Basin. Msspelt as Throssel Group.|510 Ma|||||20-MAY-20
80058|Kalkarindji Supersuite|71169|5|Briefly described|p17|Cambrian|Cambrian|Officer Basin.|508 +/- 5 Ma (Macdonald et al., 2005)|||||
80058|Kalkarindji Supersuite|71267|4|Described|GEOL_LUT_CSV files|||Of the Kalkarindji LIP. Events: Alice Springs Orogeny (450-295 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv, 100k_geologyl_lut.csv.|||Includes Milliwindi Dolerite.|||
80058|Kalkarindji Supersuite|72490|5|Briefly described|p3||||||Antrim Plateau Volcanics|||
69564|Kalkarindji Volcanic Group|65336|4|Described|Map Legend|Early Cambrian|Early Cambrian|Of Georgina Basin [?the volcanics are much more extensive than Georgina Basin - CEB OCT-2010]. Includes Helen Springs Volcanics. Unconformably overlies South Nicholson Group; unconformably underlies Narpa Group. ||||||29-SEP-11
69564|Kalkarindji Volcanic Group|65337|3|Fully described|p61 Table 6, pp94-95.|Early Cambrian|Ediacaran|Encompasses all Early Cambrian continental volcanic rocks in northern Australia. Continental extrusive, high-level intrusive units; sedimentary constituents fluviatile to lacustrine or shallow marine.|||Includes Helen Springs, Antrim Plateau, Colless  Volcanics; Jarong Conglomerate; Kinevans Sandstone; Jindare Formation; Mount Ramsay, Boondawari and Milliwindi dolerites, and more.||Partly vesicular or amygdaloidal tholeiitic basalt, dolerite and andesite; minor trachyte, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits, quartz sandstone, siltstone, conglomerate, sedimentary breccia, limestone, chert.|
69564|Kalkarindji Volcanic Group|67352|5|Briefly described|p30-31|Cambrian|Cambrian|Rawlings et al. (2008). [This name superseded by Kalkarindji Suite] Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km. Various names for exposures include Antrim Plateau, Nutwood Downs, Helen Springs, Peaker Piker, Colless and Table Hill Volcanics.|||Antrim Plateau Volcanics, Colless Volcanics, Table Hill Volcanics, Nutwood Downs Volcanics.|||
69564|Kalkarindji Volcanic Group|69445|6|Mentioned|p30:1, 3|||Kruse in Rawlings et al. (2008); included some components of the Kalkarindji Continental Flood Basalt Province in NT and WA, including minor intercalated sedimentary units. Replaced herein by Kalkarindji Suite.||||||12-JUL-16
69564|Kalkarindji Volcanic Group|69591|6|Mentioned|p54|||Camooweal-Murphy Domain.|||Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72408|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72414|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72415|4|Described|mapsheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72416|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.|||Includes Colless Volcanics.|||
75516|Kalkarindji volcanics|62557|6|Mentioned|p461|||Informal refrence to the units of the Kalkarindji continental flood basalt province - a large igneous province (LIP)||||||14-SEP-09
78640|Kalpini Dyke|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Dolerite and gabbro; includes cumulate and granophyric differentiates.|06-AUG-15
78640|Kalpini Dyke|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
78640|Kalpini Dyke|71270|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Yilgarn Craton, West Australian Craton.||Unit of Widgiemooltha Dyke Suite.|||Dolerite and gabbro; includes cumulate and granophyric differentiates|
35220|Kambalda Dome Granodiorite|23159|6|Mentioned|p794|||||||||10-SEP-19
80243|Kambalda Formation|71308|6|Mentioned|p708|||Southern Kalgoorlie Terrane.||||||
25101|Kambalda Hanging Wall basalt|40302|6|Mentioned|Fig.2|||||||||
28632|Kambalda komatiite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain.  Of the Kalgoorlie Group.  Age: 2708 +/- 7Ma (zircon).||||||07-NOV-08
28632|Kambalda komatiite|41432|6|Mentioned|p13|||||||||
28632|Kambalda komatiite|62111|6|Mentioned|p1460 Fig. 6|||Informal - see Kambalda Komatiite. See also p1462 Fig. 8.||||||07-FEB-11
40290|Kambalda komatiites|24322|5|Briefly described|p72|Neoarchean|Neoarchean|Informal-see Kambalda Komatiite Formation.  Of the Kambalda Group.||||||07-NOV-08
40290|Kambalda komatiites|70863|6|Mentioned|p11 Fig.8|||||||||
77094|Kambalda sequence|64633|6|Mentioned|p8. |||||||||
24642|Kangan Adamellite|37633|4|Described|Table 41|||See also Plate 5 and P34.||||||
24642|Kangan Adamellite|39697|3|Fully described|p38|||||||||
24642|Kangan Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||180 sq. km. Post-tectonic granitoid.||Yule Granitoid Complex|||Biotite monzogranite; syenogranite, porphyritic, foliated.|
24642|Kangan Adamellite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Superseded by Mungarinya Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
28205|Kangan Granite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
69903|Kangaroo Caves Formation, Upper|61256|6|Mentioned|p340 Fig. 5c|||Informal - see Kangaroo Caves Formation.||||||27-JAN-06
36973|Kangi Creek Formation|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
73789|Kanowna Belle porphyry|60514|6|Mentioned|p49|Archean|Archean|Informal name; see Kanowna Belle Porphyry.||||||07-FEB-11
73789|Kanowna Belle porphyry|62107|6|Mentioned|p1403|||Informal name. In the Eastern Goldfields Province.||||||
73789|Kanowna Belle porphyry|66880|6|Mentioned|p11, p29. |Archean|Archean|The formal name capitalises the Porphyry.|2655 +/- 6 Ma (Rose et al. 2004).|||Intrudes the Kalgoorlie Sequence.||
73789|Kanowna Belle porphyry|71166|5|Briefly described|p122, p126|||Hosts 70% of the mineralization at Kanowna Belle. Many gold hosting features including carbonate breccias, vein stockworks and sheeted vein arrays were formed during sinistral movement of the Fitzroy fault. |2655 +/- 6 Ma (Ross et al, 2004)|||Intrudes the Fitzroy Mylonite.|Porphyry, carbonate breccias and siliceous breccias.|
73753|Kanowna Conglomerate|63637|5|Briefly described|p12|||Overlies Ballarat Conglomerate; overlain (dis)conformably by Grave Dam Grit. Geological province: Eastern Goldfields Province. Clasts of feldspar+/-quartz-phyric dacite are present in analysed drillholes.||||||17-OCT-07
73753|Kanowna Conglomerate|70482|5|Briefly described|p319, 329|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Over 250m thick. Is presented as Kanowna conglomerate.|2655 +/- 10 Ma (MDA).|Kalgoorlie Sequence.||Conformably overlies Ballarat turbidite locally. Is overlain conformably by Kanowna turbidite. Is intruded by Red Hill Granite.|Poorly sorted, internally massive to weakly graded beds; includes porphyritic and equigranular felsic clasts, and mafic, ultramafic and volcaniclastic conglomerates.|
73753|Kanowna Conglomerate|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Black Flag Group||||
73753|Kanowna Conglomerate|73391|5|Briefly described|p51, 143, 146, 180, 187, 223, 239, 304|||See also Appendices. Used synonymously with Kanowna conglomerate, Kanowna conglomerate member or simply Kanowna member.||||Gradationally overlies Ballarat Conglomerate. Is overlain by Grave Dam Grit.|Thickly-bedded (6-58m each) polymictic conglomerate; rare sandsone and siltstone beds.|
83382|Kanowna conglomerate member|73391|5|Briefly described|p142-147, 174, 187|||Is presented as Kanowna Conglomerate, Kanowna conglomerate, Kanowna conglomerate member and Kanowna member, apparently interchangeably. Described in detail; graphic drill log, photographs, photomicrographs.||||Overlies Ballarat Conglomerate. Is overlain by Government Dam member or Grave Dam Grit.||
80210|Kanowna member|71166|5|Briefly described|p23|||[An informal, probable company name from the Kanowna gold camp]|||||Polymictic conglomerate and sandstone.|
80210|Kanowna member|73391|5|Briefly described|p132, 134, 142-148, 153, 178, 182, 194|||See also p239, 244, 282, 304. Kanowna district, Boorara Domain. Also referred to as Kanowna conglomerate member. May be part of the same depositional unit including the Ballarat member. Detailed description of lithology; graphic drill log, photographs, photomicrographs.|~2687 Ma.|Black Flag Formation. ??Talbot formation.||Gradationally overlies Ballarat member. Is overlain unconformably by Grave Dam member.|Massive section of thick-bedded polymictic conglomerate (mainly mafic volcanic and feldspar-[hornblende] porphyry clasts), surrounded by upper and lower zones of pebbly sandstone. ~650m thick.|
83950|Kanowna turbidite|70482|5|Briefly described|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.||Kalgoorlie Sequence.||Conformably overlies Kanowna Conglomerate. Is overlain (dis)conformably by Grave Dam Grit.|Feldspar-rich volcanic sandstone, siltstone and lesser mudstone.|
70732|Kanpa Beds''|62453|6|Mentioned|p32|||Informal, see Kanpa Formation.||||||
40109|Kanpa beds""|23571|6|Mentioned|p8|||Informal name - upgraded to Kanpa Formation (Cockbain and Hocking, 1989). Geological Province: Officer Basin.||||||16-MAY-05
40109|Kanpa beds""|24161|6|Mentioned|p12|||Informal - see Kanpa Formation.||||||
70733|Kanpa beds''|62453|6|Mentioned|p32|||Informal, see Kanpa Formation.||||||
79863|Kantie Murdana Volcanic Member|71159|5|Briefly described|Map legend.|Archean|Archean|Youanmi Terrane, Yilgarn Craton.||Yaloginda Formation.||||
29556|Kantie Murdana Volcanics|23787|5|Briefly described|p62|Archean|Archean|Age: 2813+3Ma (SHRIMP U-Pb).||||||07-NOV-08
29556|Kantie Murdana Volcanics|42978|6|Mentioned|Fig.1 p282|||Misspelling of Kantie Murdanna Volcanics||||||
29556|Kantie Murdana Volcanics|44149|5|Briefly described|p120, p121 Fig.2-126|Archean|Archean|||||Overlies Windimurra Complex tectonically or unconformably.|A sequence of felsic volcanics and BIF, metamorphosed to prehnite-pumpellyite or lower greenschist facies.|
29556|Kantie Murdana Volcanics|65268|5|Briefly described|p8|Mesoarchean|Mesoarchean|Overlies part of Windimurra Intrusion (roof pendants?)|2813 +/- 3 Ma (SHRIMP U-Pb zircon: Nelson, 2000)||||Felsic volcanic rocks, volcanic sandstone, BIF, chert, granophyre and dolerite.|
27946|Kantie Murdanna Volcanics|23780|5|Briefly described|p108|Archean|Archean|Age: ~2813+/-3 Ma||||||07-NOV-08
27946|Kantie Murdanna Volcanics|38492|4|Described|p17|||||||||
27946|Kantie Murdanna Volcanics|40337|4|Described|p12|||||||||
27946|Kantie Murdanna Volcanics|42010|4|Described|p172|||||||||
27946|Kantie Murdanna Volcanics|64891|5|Briefly described|p43|Archean|Archean|Overlie Windimurra Igneous Complex which has intruded these volcanics. Rhyolites.||||||07-FEB-11
27946|Kantie Murdanna Volcanics|66195|5|Briefly described|p605|Neoarchean|Mesoarchean|Rhyolite in roof pendant above Windimurra Igneous Complex provides maximum age for WIC. ?part of  Norie Group.|Crystallisation age 2813 +/- 3 Ma.|||||13-MAR-12
27946|Kantie Murdanna Volcanics|67129|6|Mentioned|p63|||||||||
27946|Kantie Murdanna Volcanics|68561|5|Briefly described|GEOCHRON files|||Murchison Domain, Youanmi Terrane. Rhyolite U-Pb zircon crystallisation age: 2813 +/- 3 Ma. Interpreted roof pendant above Windimurra Igneous Complex, hence provides a maximum age for WIC. See geochron file 194747.1.pdf.||||Interpreted to form a roof pendant above Windimurra Igneous Complex||
27946|Kantie Murdanna Volcanics|68698|5|Briefly described|p15, p27-28|||Contemporary with Mount Kenneth Suite. Considered to be genetically related to the Meeline and Boodanoo Suites. Brief geochemistry. See also reference to Kantie Murdanna Volcanics Member (p9).||||||
76185|Kantie Murdanna Volcanics Member|68698|5|Briefly described|p9|||Contemporaneous with Mount Kenneth Suite; has similar REE pattern. See also reference to Kantie Murdanna Volcanics (p15, p27-28).|2813 +/- 3 Ma.|||||
76185|Kantie Murdanna Volcanics Member|69014|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane. Age constrained by the Yaloginda Formation.|2815-2805 Ma|Of the Yaloginda Formation.|||Rhyolite and banded-iron formation, metamorphosed; psammitic and pelitic schist with abundant cordierite poikiloblasts up to 15 mm in diameter.|01-MAY-14
76185|Kantie Murdanna Volcanics Member|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Yaloginda Formation||Overlies the Mugs Luck Basalt|Felsic volcaniclastic and volcanic rocks, banded iron formation.|
76185|Kantie Murdanna Volcanics Member|69586|5|Briefly described|p22|Neoarchean|Neoarchean|Murchison Domain.||Yaloginda Formation.||||
25104|Kapal Slate|42892|6|Mentioned|Table 4|||misspelling of Kapai Slate?||||||
41234|Karalundi formation|50226|6|Mentioned|p420|||Informal - see Karalundi Formation.||||||
70734|Karara Beds''|62453|6|Mentioned|p64|||Informal Name.||||||
77185|Karara beds|44139|6|Mentioned|p282|||Of Williams and others (1976). Replaced by Karara Formation (Crowe and Chin, 1979).| | ||||05-MAR-18
40089|Karbhan Subgroup|24115|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Geological Province: Collier Basin.||||||
40089|Karbhan Subgroup|24535|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of Bangemall Grop. Rocks now incorporated in the Collier Group. Geological Province: Collier Basin.||||||26-NOV-13
34420|Karbon subgroup|22716|6|Mentioned|table4, p237|Ectasian|Ectasian|Age: 1300 Ma. Part of the Bangemall Basin succession.||||||
78078|Kardinya Shale|68254|5|Briefly described|p1036 Fig.2, p1043|Cretaceous|Cretaceous|Presented as Kardinya Shale. See Kardinya Shale Member in this paper.||Of the Osborne Formation.|||Comprises shale/siltstone.|
78078|Kardinya Shale|68811|5|Briefly described|p92 fig 52, p180 tbl 39|Cretaceous|Cretaceous|||||Overlies the Leederville Formation. Overlain by the Lancelin Formation.|Siltstones, shales and sandstone.|
70224|Karloning pegmatite|24410|6|Mentioned|p169 Tables 72|||Informal name. ||||||
42506|Karmt Shoals|24206|5|Briefly described|p230, p227 Fig. 1|||In the Northwest Shelf area.  Geological Province: Nancar Trough.||||||
77656|Karramindie granitoid|68066|6|Mentioned|p28|Archean|Archean|Discussed by Oversby (1975). See also Karramindie Monzogranite||||||29-NOV-12
34940|Karratha Granite|22953|6|Mentioned|Fig1p3|||||||||
34940|Karratha Granite|44150|6|Mentioned|p130-131 Fig.2-130|||||||||
40064|Karratha Granitoid|23936|5|Briefly described|p3|Archean|Archean|Age: ca. 3270 Ma. Geological Province: Pilbara Craton. Informal - see Karratha Granitoid Complex.||||||07-NOV-08
40064|Karratha Granitoid|24391|5|Briefly described|p8-2|Archean|Archean|Age: 3270-3260 Ma (U-Pb). Massive, medium grained granodiorite-tonalite. Geological Province: Pilbara Block.||||||07-NOV-08
38557|Karratha Granitoid Complex|23813|6|Mentioned|p91 Tb. 1|Archean|Archean|Age: 3.26Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
38557|Karratha Granitoid Complex|23936|5|Briefly described|Tb.1|Archean|Archean|Age: ca. 3.26 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
38557|Karratha Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||West Pilbara. Poorly exposed.|||||Foliated monzogranite, granodiorite, migmatite; some porphyritic phases.|
70436|Karratha Stone|61273|5|Briefly described|p85|Archean|Archean|Not a formal stratigraphic name - commercial name for dimension stone quarried from the Hardey Formation in the Pinderi Hills. Quartzose flagstones of red-brown sandstone - with colour variations from cream to brown, light green, and pink.||||||07-NOV-08
67864|Karrawang Formation|60076|5|Briefly described|p13|Archean|Archean|Probably a misspelling of Kurrawang Formation.  Along with the Merougil Conglomerate these are the uppermost of the Kalgoorlie greenstones, comprising rudaceous and arenaceous sedimentary rocks.||||||07-NOV-08
41214|Karri Karri member|50223|6|Mentioned|p346|||Informal - see Karri Karri Member.||||||
41214|Karri Karri member|50224|6|Mentioned|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Informal name.  Of the Chiall Formation (Minningarra Subgroup).||||||07-FEB-11
37895|Kathleen Valley Gabbro""|24135|6|Mentioned|p13|||Informal - see Kathleen Valley Gabbro.||||||
37197|Kathleen Valley gabbro complex|23611|6|Mentioned|p11|||||||||
25109|Kathleen Valley granite""|33558|5|Briefly described|p157|||Stratigraphy||||||
38635|Katrine Syenite|23785|5|Briefly described|p9|Archean|Archean|Age: 2654+/-5Ma.  Geological Province: Yilgarn Craton.||||||07-NOV-08
70637|Kavir suite|61252|6|Mentioned|p67 Tb.1|||Informal name. Of the Yule granitoid complex.||||||
75099|Kellerberrin Granite|64769|6|Mentioned|p31 Tb. 4, p33|||Name for dimension stone - not intended as a formal name. Light-medium grey and medium-grained granite. In WA.||||||16-APR-09
39987|Kelley Subgroup|24184|6|Mentioned|p699 Fig.3|Archean|Archean|Misspelt - see Kelly Subgroup. Parent: Warrawoona Group. Underlying Unit: Salgash Subgroup. Geological Province: Pilbara Craton.||||||07-NOV-08
39987|Kelley Subgroup|50427|4|Described|p182 Fig.5|Archean|Archean|Age: 3430-3320 Ma, Unconformably overlies Coonterunah Group, Talga Talga Subgroup and Salgash Subgroup (some contacts conformable). Overlain unconformably by Budjan Creek Formation and conformably by Golden Cockatoo Formation. Of Warrawoona Group.||||||07-NOV-08
39987|Kelley Subgroup|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
73255|Kelly Group basalts|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Informal reference to undivided basalts of the Kelly Group. Geological Province: Pilbara Craton.||||||07-NOV-08
39986|Kelly Subgroup|24184|5|Briefly described|p701|Archean|Archean|Of the Warrawoona Group. Underlain by Salgash Subgroup. Geological Province: Pilbara Craton. See also Kelley Subgroup. Newly defined as uppermost unit of the Warrawoona Group, includes Euro Basalt and Wyman Formation||||||07-NOV-08
39986|Kelly Subgroup|24531|5|Briefly described|p5|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
39986|Kelly Subgroup|24590|5|Briefly described|p32|Archean|Archean|Newly formed subgroup of the Warrawoona Group. Now contains the Euro Basalt and Wyman Formation.||||||07-FEB-11
39986|Kelly Subgroup|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Warrawoona Group.  Includes: Euro Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
39986|Kelly Subgroup|50381|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
39986|Kelly Subgroup|50544|5|Briefly described|p18, p24|Archean|Archean|Newly proposed (Bagas, 2003) third subgroup of the Warrawoona Group, to include the Euro Basalt, formerly of the Salgash Group.||||||07-NOV-08
39986|Kelly Subgroup|50555|5|Briefly described|Map legend|Archean|Archean|Of the Warrawoona Group.  Includes the Euro Basalt.  Geological Province: Pilbara Craton.||||||07-NOV-08
39986|Kelly Subgroup|61253|5|Briefly described|p51|Archean|Archean|Superseded by Kelly Group (Pilbara Supergroup). Formerly contained Strelley Pool Chert, Euro Basalt, Wyman Formation and Charteris Basalt which have remained assigned to the Kelly Group. Geological Province: Pilbara Craton.||||||09-DEC-08
39986|Kelly Subgroup|63441|5|Briefly described|p4 Tb. 1, p6 Tb. 1|Archean|Archean|Redefined as Kelly Group (Pilbara Supergroup). Formerly within the Warrawoona Group.||||||07-FEB-11
39986|Kelly Subgroup|64328|4|Described|p54, p57|||Of the Warrawoona Group. Contains Euro Basalt, Wyman Formation, and Charteris Basalt. Conformably overlies the Salgash Subgroup.||||||07-FEB-11
39986|Kelly Subgroup|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Warrawoona Group. Includes Euro Basalt, Wyman Formation and Charteris Basalt. Geological Province: Pilbara Craton.||||||07-FEB-11
39986|Kelly Subgroup|64936|5|Briefly described|map legend|Archean|Archean|Of Warrawoona Group. Includes Wyman Formation, Euro Basalt and Strelley Pool Chert. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
39986|Kelly Subgroup|65008|5|Briefly described|p5, p7, p8 Fig.5, p9, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Redefined by Bagas et al. (2004a) to include the Euro Basalt, Wyman Formation, Strelley Pool Chert, and Charteris Formation.|3350-3315 Ma|Of the Warrawoona Group|Includes Charteris Basalt, Wyman Formation and Euro Basalt.|||
39986|Kelly Subgroup|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3325 - 3315 Ma (Buick 2002).|Of Warrawoona Group. |Includes Charteris Basalt, Wyman Formation and Euro Basalt.|||
39986|Kelly Subgroup|65825|6|Mentioned|p5. |Archean|Archean|Formerly a unit in the Warrawoona Group. Promoted to Group status by Van Kranendonk et al. (2004) to include all rocks formerly assigned to the Warrawoona Group. Changes are detailed in Appendix 2 of the report.||||||
39986|Kelly Subgroup|65827|6|Mentioned|p6 Tb.1, p20|||Of Warrawoona Group; former name of Kelly Group.
||||||
39986|Kelly Subgroup|65828|6|Mentioned|Map legend|Archean|Archean|||Unit in Warrawoona Group.|Includes Euro Basalt.|||
39986|Kelly Subgroup|66217|6|Mentioned|p8.  |||Van Kranendonk et al. (2002) included the Euro Basalt, Wyman Formation and Charteris Basalt in this unit in their redefinition of the Warrawoona Group. Elevated to Group status by Van Kranendonk et al. (2006a, 2007) on the basis of a regional unconformity beneath Strelley Pool Chert.||||||
28640|Kellys Knob Member|32870|6|Mentioned|Fig.11|||Refers Veevers (1969).||||||04-OCT-06
28640|Kellys Knob Member|41811|6|Mentioned|p210|||||||||
28640|Kellys Knob Member|45038|14|Not recorded|p.17,18|||See also Figures and Plates.||||||04-OCT-06
28640|Kellys Knob Member|45039|6|Mentioned|p5|||Upper Devonian||||||
28640|Kellys Knob Member|45040|14|Not recorded|p5, fig.2||Late Devonian|(Upper Devonian). Pt. Cockatoo Formation.||||||
28640|Kellys Knob Member|45041|6|Mentioned|Fig.45|||Dev. Cockatoo Fm.||||||
28640|Kellys Knob Member|45050|6|Mentioned|p7|||See also pp8,9,12-14 etc. Late Frasnian||||||04-OCT-06
28640|Kellys Knob Member|45063|6|Mentioned|p12|||See also Fig. 3. Frasnian.||||||04-OCT-06
32806|Kellys Member|45038|14|Not recorded|Fig 4|||||||||
32763|Kennedy Sandstone|24044|6|Mentioned|p539|||Superseded by Kennedy Group.||||||
32763|Kennedy Sandstone|45015|6|Mentioned|p8|||Of Raggatt (1936). Equated with Tumblagooda Sandstone by Forman (1937).||||||29-JAN-08
32763|Kennedy Sandstone|45016|14|Not recorded|p.176|||Ref.to Condit 1935, p.870.||||||
42391|Kennedy Stage""|23815|6|Mentioned|p288|||Supersed by the Kennedy Group (Condon, 1954).||||||
83813|Kent Complex|73631|5|Briefly described|p2, p3 Fig.1C|Archean|Archean|Yilgarn Craton. Occurs NE of the Teutonic Bore VHMS Camp.||Penzance Supersuite.|Penzance granite.|Bounded to the east by the Teutonic Bore volcanic complex.|A large composite batholith of HFSE granitoid intrusions.|
81305|Kent Complex granite|70020|6|Mentioned|p122|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.|2679+\-8 Ma|||||
41113|Kent granite|24196|5|Briefly described|p70|Archean|Archean|Informal name. Age: 2686 +/- 7 Ma (SHRIMP U-Pb: Black et al., 2002). Geological Province: West Malcolm sub-domain, Yilgarn Craton.||||||07-NOV-08
38667|Kent syenogranite|23786|5|Briefly described|p60|||Informal name. Geological Province: Yilgarn Craton.||||||
38667|Kent syenogranite|24196|5|Briefly described|p44|Archean|Archean|Informal name. Age: 2686 +/- 7 ma (Black et al., 2002).||||||07-NOV-08
72625|Keraudren Formation, Lower|13255|5|Briefly described|p376|Early Triassic|Early Triassic|Part of the Westralian 1 petroleum super-system: discussed in detail. See also reference to Keraudren Formation (p369).|||||Deltaic sands.|
72625|Keraudren Formation, Lower|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Middle Triassic|Age: ~240-~235Ma. Geological Province:  Bedout Sub-basin (Roebuck Basin).||||||
72625|Keraudren Formation, Lower|67368|6|Mentioned|p209 Fig.4.|Middle Triassic|Early Triassic|||||||
72625|Keraudren Formation, Lower|69297|5|Briefly described|p337, p339, p352|Ladinian|Anisian|Roebuck Basin. Shale and minor coal intervals are prospective hydrocarbon source rocks. ||||Overlies the Locker Shale. Overlain by the Cossigny Member.|Shale and minor coal.|
72625|Keraudren Formation, Lower|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p5|Ladinian|Anisian|Rowley Sub-basin, Roebuck Basin. Transgressive shales are potential oil- and gas-prone source rocks.||||Overlies Locker Shale. Is overlain by Cossigny Member.||
72626|Keraudren Formation, Upper|62837|5|Briefly described|Stratigraphic columns|Late Triassic|Middle Triassic|Age: ~233-~220Ma. Geological Province:  Bedout Sub-basin (Roebuck Basin).||||||07-NOV-06
72626|Keraudren Formation, Upper|69297|5|Briefly described|p337, p339, p352|Norian|Norian|Canning and Roebuck Basins. Shale and minor coal intervals are prospective hydrocarbon source rocks. ||||Overlain by the Bedout Formation. Overlies the Cossigny Member.|Shale and minor coal.|
72626|Keraudren Formation, Upper|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p5|Rhaetian|Carnian|Roebuck Basin and offshore Canning Basin. Coaly shales are potential source rocks.||||Overlies Cossigny Member. Is overlain by Bedout Formation.||
75822|Kerba Granodiorite|65269|6|Mentioned|p38|||Used as an internal reference material by GSWA for geochemical analyses||||||
79865|Kestral Cavern Gabbro|71165|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Moodini Supersuite.|||Monzogabbro to leucogabbro.|
34456|Kevin Dams Monzogranite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
41456|Kevins Dam Granite|50437|6|Mentioned|p4.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Kevins Dam Suite (Sally Downs Supersuite). Used interchangeably with Kevins Dam Monzogranite.||||||07-NOV-08
37108|Kevins Dam suite|23751|5|Briefly described|p16|Orosirian|Orosirian|Age: c.1810-1800 Ma. Of Sally Downs supersuite.||||||
37108|Kevins Dam suite|66845|4|Described|p537 Fig.3, p538, p539, p543|||Mount Christine Granitoid (older and younger portions) are assigned to two different parents (Syenite Camp Suite and Kevins Dam suite, respectively) in Tb1. SHRIMP U-Pb zircon dating results. Analysed samples vary into two age groups and many plutons are undated. These two groups cannot be discriminated chemically, thus placed into one suite.||Sally Downs supersuite|Mount Christine Granitoid (younger) and Loadstone Monzogranite||mainly massive, medium-grained, even-textured and porphyritic biotite monzogranite and syenogranite; mafic enclaves|
37108|Kevins Dam suite|66846|4|Described|p549-552, p554, p556-559, p548 Fig.1|Orosirian|Orosirian|Age range probably from U-Pb SHRIMP dating of zircon (see p547). Rare earth element abundances given on p551 Tb. 2.|1831-1805|Sally Downs supersuite|||Biotite monzogranite and syenogranite; porphyritic textures common; massive.|
37108|Kevins Dam suite|72437|4|Described|p9, p11, p102, p111|Palaeoproterozoic|Palaeoproterozoic|Intrusions intrude all three zones of the Lamboo Complex, but primarily the central zone. O'Brien (1994) provided four analyses from the Koondooloo Monzogranite. Also includes  Shepherds Bore Granite, Loadstone Monzogranite, Violet Valley Tonalite.|c. 1815-1800 Ma|Sally Downs supersuite|Includes the Koondoloo Monzogranite, Dillinger Monzogranite, Mount Christine Granitoid, Magotty Springs Monzogranite and Wesley Yard Monzogranite.||Massive monzogranite and syenogranite intrusions.|
77744|Khyalla Formation|64975|6|Mentioned|pp161-162.|Mesoproterozoic|Mesoproterozoic|Mis-print of Kyalla.||||||
37204|Kialrah rhyolite|23793|6|Mentioned|p28|||Informal - see Kialrah Rhyolite||||||10-SEP-19
75070|Kiangi Formation|64728|5|Briefly described|p95 Fig.2.|||Replaced by Kiangi Creek Formation.|Contains detrital zircons clustered  c.1800 Ma.|Unit in Edmund Group.||||
29246|Kidson beds|45153|2|Defined|App.8-139|Aptian|Aptian|Also referred to as Anketell Formation (Playford & others, 1975.)||||||
41114|Kilkenny gabbro|24196|6|Mentioned|p70|||Informal name. Geological Province: North Murrin sub-domain, Yilgarn Craton.||||||
70465|Killara Formation, upper|62094|6|Mentioned|p236|||Informal - see Killara Formation.||||||
75988|Killarra Formation|12099|6|Mentioned|p678 Fig.4|||Misspelling of Killara Formation, Mooloogool Subgroup, Yerrida Group.||||||
75988|Killarra Formation|70804|5|Briefly described|p2, p13, p37|||New name. Misspelt as the Killara Formation on p13, p37.||Mooloogool Subgroup|Includes the Bartle Member.|||28-FEB-23
34410|Killi Killi beds|22496|5|Briefly described|p9|||Probably correlative of the Olympio Formation.  Overlain unconformably by Gardiner Sandstone.||||||
34410|Killi Killi beds|22716|6|Mentioned|table4, p229|Orosirian|Orosirian|||||||
34410|Killi Killi beds|23621|6|Mentioned|p16|||Of Tanami Complex.||||||
34410|Killi Killi beds|24173|5|Briefly described|p17|||Of the Tanami Complex. In the Granites-Tanami region. Age: c.1850Ma. Possible correlation with younger turbidites of Olympio Formation||||||06-APR-05
34410|Killi Killi beds|61861|6|Mentioned|p3 Table 1. |Paleoproterozoic|Paleoproterozoic|Of Blake et al (1979).||Unit in Tanami Complex.||||
34410|Killi Killi beds|63261|6|Mentioned|p11, p13|||Informal name of Blake et al (1972). Parts mapped by Hodgson (1976) and Hendrickx (200b) as the former Killi Killi beds.||||||07-FEB-11
34410|Killi Killi beds|64329|5|Briefly described|p20|||Unconformably underlies Gardiner Sandstone. Steeply dipping basement shales and greywackes.||||||29-JUL-08
34305|Kimberley Block|22683|6|Mentioned|93|||Geological province, not stratigraphic name.||||||
79598|Kimberley Dyke Suite|70761|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|North Australian Craton.||||||10-NOV-16
79598|Kimberley Dyke Suite|70826|6|Mentioned|p14 tbl 5|Proterozoic|Proterozoic|Kimberley. Age ranges from 2500-541 Ma [not very useful].||||||20-MAY-20
79598|Kimberley Dyke Suite|71267|4|Described|GEOL_LUT_CSV files|Carboniferous|Devonian|Events: Western Australian events (4000-0.01 Ma); North Australian Craton events (2500-250 Ma); Alice Springs Orogeny (450-295 Ma). See 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|419.2-298.9 Ma (inferred)||||Dolerite; typically northeasterly trending dykes|
79230|Kimberley Group, Lower|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|King Leopold Sandstone, Carson Volcanics.|||
79230|Kimberley Group, Lower|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|King Leopold Sandstone, Carson Volcanics.|||
79230|Kimberley Group, Lower|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|King Leopold Sandstone, Carson Volcanics.|||
79230|Kimberley Group, Lower|70812|5|Briefly described|p6|Statherian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1800 Ma|Kimberley Group|Includes the King Leopold Sandstone, Carson Volcanics and the Warton Sandstone.|||
79230|Kimberley Group, Lower|70851|4|Described|p4-p6, p17-p20|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Misspelt as the Kimberley Subgroup, Lower on p4. |c. 1800-1775 Ma||Includes the King Leopold Sandstone, Carson Volcanics and the Warton Sandstone.|Unconformably overlies the Speewah Group. Overlain by the Kimberley Subgroup, Upper.||
79230|Kimberley Group, Lower|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. Informal name.||||||
79231|Kimberley Group, Upper|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|Warton Sandstone and Pentecost Sandstone, Elgee Siltstone.|||04-NOV-15
79231|Kimberley Group, Upper|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|Warton Sandstone, Elgee Siltstone, Pentecost Sandstone.|||
79231|Kimberley Group, Upper|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|Warton Sandstone, Elgee Siltstone, Pentecost Sandstone.|||
79231|Kimberley Group, Upper|70812|5|Briefly described|p6|Statherian|Statherian|Western Zone of the Halls Creek Orogen, Lamboo Province.|c. 1775 Ma|Kimberley Group|Includes the Elgee Sandstone and Pentecost Sandstone.|||
79231|Kimberley Group, Upper|70851|5|Briefly described|p4-p6, p17-p19, p29|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Misspelt as the Kimberley Subgroup, Upper on p4.|c. 1775-1750 Ma|||Overlies the Carson Volcanics. Overlain by the Bastion Group.||
79231|Kimberley Group, Upper|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. Informal name.||||||
69629|Kimberley Pearl granite|61273|6|Mentioned|p87|||Not intended as a formal stratigraphic name. Commercial name for a lustrous grey dimension stone from Western Australia||||||
33175|Kimberley Plateau "Series"|44479|2|Defined|opp.p.6, Tb.1|||E/51-1. Correlated with the Upper Proterozoic of this Sheet.||||||
69626|Kimberley Quartzite|61273|5|Briefly described|p85|Early Cretaceous|Early Cretaceous|Not intended as a formal name - commercial name for dimension stone quarried from the Melligo Sandstone.   Fine-grained, thinly bedded.||||||17-MAY-06
69626|Kimberley Quartzite|64769|6|Mentioned|p7|||Pale beige stone. WA.||||||06-MAY-09
69625|Kimberley Sandstone|61273|5|Briefly described|p85|Early Cretaceous|Early Cretaceous|Not intended as a formal name - commercial name for dimension stone quarried from the Melligo Sandstone.  Fine-grained, thinly bedded.||||||17-MAY-06
26664|King Leopold Beds|29549|5|Briefly described|p201|||||||||
26664|King Leopold Beds|31446|4|Described|p6|||Refers to Guppy et al., (1958). SD51-15,16.||||||
26664|King Leopold Beds|38263|6|Mentioned|p9|||||||||
26664|King Leopold Beds|39796|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26664|King Leopold Beds|44363|14|Not recorded|p.12|||Now known as Speewah Group.||||||
26664|King Leopold Beds|44994|6|Mentioned|Fig.4|||||||||
26664|King Leopold Beds|44998|14|Not recorded|p15,101|||||||||
26664|King Leopold Beds|48837|14|Not recorded|p.26|||||||||
25124|King Leopold sandstone|41453|6|Mentioned|Fig.1|||||||||
25124|King Leopold sandstone|41987|6|Mentioned|Fig.9 P78|||||||||
83874|King of the Hill Dyke|68471|6|Mentioned|p14|||Palaeomagnetic declinations and inclinations tabulated.||||||
79235|King of the Hills Dolerite|70773|4|Described|p65|Proterozoic|Proterozoic|Proterozoic age is derived from cross-cutting relationships. SHRIMP ages are derived from D Mole (Unpublished) and are interpreted as inherited, this is supported by the rounded morphology of the zircons. Outcrops over a strike length of around 80km between Sturt Meadows Homestead in the west and Charlie Bore in the east (see text for coordinates). Outcropping inferred from aeromagnetics. Petrography is discussed briefly on p66.|c. 2595, 2628 and 2730 |Widgiemooltha Supersuite|||Dolerite/diorite dyke with abundant xenoliths.|
79235|King of the Hills Dolerite|71270|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Of the Widgiemooltha Large Igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420 - 2400 Ma).|2420-2400 Ma (inferred)|Unit of Widgiemooltha Supersuite.|||Dolerite with abundant felsic xenoliths|
32888|King's Park Shale|48848|14|Not recorded|p.22-27,29-34|||||||||
83357|Kingia Sandstone''|73117|6|Mentioned|p15|Artinskian|Artinskian|[Written as 'Kingia Ss'; may represent informal usage?].||||Underlain by and equivalent to[?] High Cliff Sandstone.||
38591|Kingston Ultramafic|23782|5|Briefly described|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
32576|Kingswood Basalt|45543|4|Described|p.101,102||Archean|Lowest unit of Woolyeenyer Group.||||||07-NOV-08
80353|Kirby Range Member|70774|5|Briefly described|p9|Wuchiapingian|Wuchiapingian|||Hardman Formation.||Overlies the Condren Sandstone. Overlain by the Hicks Range Member.||10-FEB-20
67867|Kirgella banded gneiss|60076|6|Mentioned|p24|Archean|Archean|Not intended as a formal name.  Quartz-feldspathic rocks.||||||07-NOV-08
77437|Kirkby Radiolarite|60386|5|Briefly described|p297|Lopingian|Guadalupian|Roebuck/Canning Basin. Limestone nearshore-shelf.||Of Liveringa Group.||||
29655|Kirkby Range Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
29655|Kirkby Range Sandstone|64974|6|Mentioned|p148 Fig. 6|Tatarian|Tatarian|Of Hardman Formation. Geological Province: Canning Basin.||||||24-JUN-09
25126|Kirup Conglomerate""|29693|6|Mentioned|p34|||||||||
25126|Kirup Conglomerate""|33747|6|Mentioned|p1076|||||||||
25126|Kirup Conglomerate""|37341|6|Mentioned|p245|||||||||
78496|Kitty's Gap Chert|67668|5|Briefly described|p.161.||Paleoarchean|Informal. 'Kitty's Gap Chert'. Found in the Coppin Gap greenstone belt towards the northeast of the East Pilbara Terrane (see Westall et al. 2006). Includes putative microfossils (spheroids, filaments and rods).||Panorama Formation (Warrawoona Group)|||Silicified volcaniclastic sediment.|
78496|Kitty's Gap Chert|70729|6|Mentioned|p176|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Coeval with Apex chert.||||||
74138|Kittys Gap Chert|60636|3|Fully described|p11, p71-77|||Silicified sedimentary sequence at the top of the Kittys Gap volcano-sedimentary complex, distinguishable as lower and upper cherts. Of the Panorama Formation? See also p35-36 Fig. 3.2 and p81 for type section details.||||||07-FEB-11
74138|Kittys Gap Chert|62427|5|Briefly described|p3 Fig.2|||||Unit in Panorama Formation.|||Silicified sediment.|
74138|Kittys Gap Chert|64405|5|Briefly described|p14|||Of de Vries (2004). Informal name for chert at Kittys Gap; geochronological data suggest consistency with this unit being part of the Strelley Pool Formation. Thickness:40m. Mainly  extensively silicified volcaniclastic sandstone, siltstone, and shale.||||||07-FEB-11
74138|Kittys Gap Chert|64628|4|Described|p173 Fig.3, p177 Fig.4, p178 Fig.5.|Early Archean|Early Archean|See also Kittys Gap chert. Results of optical and scanning microscopy, analytic spectroscopy and electron microprobe are detailed and discussed.|3.46 Ga.|Unit in Panorama Formation.|||Cherts and sandstones. Ca. 10mm thick black, grey, white and translucent chert laminae.|
74138|Kittys Gap Chert|73160|6|Mentioned|p16|Paleoarchean|Paleoarchean|Pilbara Craton.|3.46 Ga|||||
77521|Kittys Gap chert|64628|4|Described|p169, pp170-178. |Early Archean|Early Archean|See also Kittys Gap Chert. This unit's dacitic precursor was similar to Duffer Formation dacites. Had initial porosity up to 85 vol%. Part of an eponymous volcano-sedimentary complex in the central part of the Coppin Gap greenstone belt, Pilbara Craton; consists of massive rhyolites and quartzose sedimentary rocks. Volcaniclastic sediments were silicified during sedimentation and diagenesis; mm-scale chert laminae were deposited through suspension settling. Results of optical and scanning microscopy, analytic spectroscopy and electron microprobe are detailed and discussed.|3446 +/- 5 Ma (De Vries et al. 2006b).|Unit in Panorama Formation.|||Cherts and sandstones; c. 10mm thick black, grey, white and translucent chert laminae.|
77521|Kittys Gap chert|70834|6|Mentioned|p312|Paleoarchean|Paleoarchean|"Appears as Kitty's Gap chert. Has vermiculite (""hydro-muscovite"") as a common alteration product of both biotite and K-feldspar."|3.45 Ga.|Panorama Formation.||||
80281|Kiwirrikurra Formation|70839|6|Mentioned|p329|Mesoproterozoic|Mesoproterozoic|Of Amadeus Basin. Outlier in the Arunta region.||||Overlain unconformably by Heavitree Quartzite.||
80281|Kiwirrikurra Formation|71080|6|Mentioned|p30 fig 21|Mesoproterozoic||Underlies Amadeus Basin in WA.|||||Dominantly sandstone.|
80281|Kiwirrikurra Formation|71088|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.||||Unconformably overlain by the Heavitree Quartzite.||
79830|Kiwirrkura Formation|69031|5|Briefly described|p4, p6 Fig.4, p8|||Warumpi Province, Arunta Orogen. Crops out in the Pollock Hills, W of Kiwirrkura. Sediment was sourced locally from Pollock Hills Formation (previously thought to include this unit). Geochronology by Kirkland et al. (2000). Place name Kiwirrkurra spelt correctly in most figures.|1570 +/- 22 Ma (maximum depositional age).||||A succession of red-weathering lithic sandstone, quartz sandstone, and conglomerate.|19-JUN-17
31380|Knobby Limestone|43563|6|Mentioned|Fig.5,p10||Late Devonian|Misspelling/variation of Knobby Sandstone||||||
38829|Kochatea Shale|24058|6|Mentioned|p111|||Misspelt - see Kockatea Shale.||||||
31939|Kojarena sandstone|43876|14|Not recorded|p581||Middle Jurassic|||||||
73565|Kooalup Limestone|63454|6|Mentioned|p76|||||||||24-JAN-08
72459|Kookynie Granite|73391|6|Mentioned|Appendices.|||Mentioned in Drill Logs Appendix.||||||
81306|Kookynie Supersuite|70020|6|Mentioned|p113,122|||Geological province: Yilgarn Craton.||||||
81306|Kookynie Supersuite|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Eastern Goldfields Superterrane.|||||HFSE-enriched granites.|
36118|Koolyanobbing Complex|23441|6|Mentioned|p163|||felsic volcanic rocks from Koolyanobbing. Not a formal name.||||||
36118|Koolyanobbing Complex|69740|6|Mentioned|p663-664|Mesoarchean|Mesoarchean|Stratigraphic columnar section.||||||
41215|Koolyin Hills quartzite|50220|5|Briefly described|p291, p292 Tb.2|||Not intended as a formal name.||||||
41215|Koolyin Hills quartzite|50223|5|Briefly described|p356|Paleoproterozoic|Paleoproterozoic|Informal name referring to quartzite of the Carrandibby Inlier, Glenburgh Terrane.  Age: 2290-2270Ma (Kinny et al, 2002).||||||01-MAR-10
75238|Koongaling Member|60373|6|Mentioned|p164|||Of Thorne and Hickman, 1998.||||||23-JUN-09
36898|Koongaling Volcanics""|23594|6|Mentioned|p13|||Mostly replaced by Hardey Formation except the rhyolite, rhyodacite and dacite component which is now Koonaling Volcanic Member of Hardey Formation.||||||
36898|Koongaling Volcanics""|23745|6|Mentioned|p10|||See Koongaling Volcanic Member of the Hardey Formation.||||||
36898|Koongaling Volcanics""|23746|6|Mentioned|p14|||Renamed Koongaling Volcanic Member. Of Fortescue Group.||||||
79263|Koongaling volcanics|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton. Mount Roe Basalt and Koongaling volcanics shown together with single age range in Fig.11. [lower case volcanics is informal use of unit name]|~2780-2760Ma Mount Roe Basalt/Koongaling volcanics|Fortescue Group||||14-DEC-16
68888|Koongee Park Formation|61056|5|Briefly described|p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Misspelt - see Koongie Park Formation. Age: 1840+/-4Ma and 1845+/-2Ma volcanics.||||||07-NOV-08
23704|Koongie Park Member|23383|6|Mentioned|p9|||Name proposed for felsic and mafic volcanic rocks and associated metasedimentary rocks which had been regarded as part of Biscay and Olympio Formations. Now raised to formation status (K.P.Formation) distinct from the Tickalara Metamorphics.  Age:1843 Ma.||||||25-JAN-05
23704|Koongie Park Member|23621|6|Mentioned|p53|||Of Ticklara Metamorphics.||||||
23704|Koongie Park Member|42768|6|Mentioned|p6|||refers to Griffin & Tyler (1992).||||||
23704|Koongie Park Member|60724|4|Described|p11|||Of Tickalara Metamorphics.Dominated by felsic volcanic and volcaniclastic material, including flow-banded rhyolite, spherulitic lavas and volcaniclastic sed. rocks; BIF recognised in parts; carbonate matrix not uncommon.Overlies Biscay Fm (Halls Creek Gp)||||||
41458|Koongie Suite|24197|6|Mentioned|p86|||Abbreviated version of Koongie Park Suite. Geological province: Kimberley Province.||||||07-FEB-11
41458|Koongie Suite|50437|6|Mentioned|p1.2|||Geological Province: Kimberley Region. Used interchangeably with Koongie Park Suite.||||||10-AUG-04
77468|Korojon Formation|12491|6|Mentioned|p454 Fig.7.|Late Cretaceous|Late Cretaceous|Presented in figure as Korojon, Withnell, Toolonga Formations. Carbonates.||||||06-NOV-14
77088|Korojong Calcarenite|6876|6|Mentioned|p100 Fig.5.|Late Cretaceous|Late Cretaceous|||||||
70735|Kukial Sandstone|62453|6|Mentioned|p16|||Overlain by Dean Quartzite.||||||
33919|Kulele Creek Formation|7161|6|Mentioned|p99 Fig.9|||Earaheedy Basin. Less than 900m thick (from p99 Fig.9).|||||Shallowing-upward packages 50m thick of siliciclastic mudstone and sandstone, oolitic-pisolitic bank carbonate, stromatolitic bioherm and breccia, and lagoonal mudstone.|02-MAY-12
33919|Kulele Creek Formation|22493|5|Briefly described|p99 Fig.9|||||||||
33919|Kulele Creek Formation|23589|5|Briefly described|p3|||Of Miningarra Subgroup. Overlain by Mulgarra Sandstone. Underlain by Wongawol Formation. In the Earaheedy Basin.||||||06-AUG-08
74622|Kulele Formation|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Minningarra Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Platform carbonate succession with stromatolites.||||||07-FEB-11
41216|Kulele formation|50223|6|Mentioned|p346|||Misspelt and informal - see Kulele Limestone.||||||
34435|Kulgera dyke swarm|22716|6|Mentioned|p238|Stenian|Stenian|Age: 1080 Ma.||||||
34435|Kulgera dyke swarm|44114|6|Mentioned|p341|||This has a very similar age to the Stuart dyke swarm 500km to the north. Appears as Alcarra (Kulgera) dyke swarm.||||||
34435|Kulgera dyke swarm|69003|6|Mentioned|p48 Fig.57|||Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.||||||
40092|Kulgera suite|24115|5|Briefly described|p30|Mesoproterozoic|Mesoproterozoic|Age: c. 1070 Ma||||||
73604|Kulgera suite granitoids|63465|6|Mentioned|p554 Tb. 1|Mesoproterozoic|Mesoproterozoic|Informal name.  Age: 1185+/-5Ma. Includes charnokites.||||||27-SEP-07
77452|Kulka Dolerite|67354|5|Briefly described|p102 Fig.33.|Permian|Permian||293 +/- 3 Ma (K/Ar 1984).|||||
74604|Kullal Dyke Suite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1000Ma. Consists of fine-grained; olivine and plagioclase porphyritic dolerite and meta-dolerite; typically porphyritic texture or granoblastic where metamorphosed.||||||
74604|Kullal Dyke Suite|65693|5|Briefly described|pp1, p3, p9, pp13-14 Figs. 11-13.|||Similar age, geographic range and structural trend to rocks of Alcurra Suite, and common within the area of mineralized gabbro.|c.1000 Ma.|||||22-APR-20
74604|Kullal Dyke Suite|65833|5|Briefly described|p17|Stenian|Cryogenian|Fine-grained olivine and plagioclase porphyritic dolerites. Typically NE trending. Cross-cuts ~1078 Ma Giles intrusions and is cut by 825 Ma Gairdner dykes. Poorly constrained Sm-Nd mineral isochron age of 1000 Ma. Also called Kullal dykes.||||||
74604|Kullal Dyke Suite|66282|5|Briefly described|Map legend.||||c.1000 Ma.||||Fine-grained olivine-plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed.|
74604|Kullal Dyke Suite|67375|5|Briefly described|pp8-9, p20 Fig.11, pp54-55, p249, p349.|||Mainly NE-trending. Chemically more primitive than many other suites: high MgO (9 to 13 %) and Ni (132-291 ppm).|?1074-?825 Ma.|||Crosscuts layered gabbro of the Giles Suite in the Hinckley Range. Is crosscut by the Gairdner Dolerite.|Fine-grained olivine-plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed.|11-DEC-13
74604|Kullal Dyke Suite|67553|5|Briefly described|p11,21,56,78-79|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Age constrained between minimum age of massive Giles gabbro (G2) and the 824+\-4 Ma emplacement age of the Gairdner Dyke Swarm (Glikson et al., 1996). Crosscut by the c. 825 Ma Gairdner Dolerite.|c. 1000 Ma||||Fine-grained olivine and plagioclase porphyritic dolerites.|
74604|Kullal Dyke Suite|69091|5|Briefly described|p54 Fig.4.2, p77-78|||Also shortened to informal Kullal dyke on p78. Age: poorly constrained Sm-Nd mineral isochron age of 1000 Ma was obtained on an olivine-bearing dyke (Glikson et al., 1996).|c. 1000 Ma|||Is crosscut by Gairdner Dolerite.|Fine-grained olivine- and plagioclase-porphyritic dolerite dykes.|
74604|Kullal Dyke Suite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194759.1.pdf||Mesoproterozoic|Paterson Orogen. GEOCHRON (SHRIMP-A U/Pb) dolerite dyke sample. 1372+/-14 Ma (4 analyses) interpreted as age of inherited component incorporated into dyke magma; provides a maximum age for crystallization.|1372+/-14 Ma|||Cross-cuts Warakurna Supersuite; is cross-cut by Gairdner Dolerite dykes.|Fine-grained olivine-plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed|02-SEP-14
74604|Kullal Dyke Suite|69436|5|Briefly described|p21:3, 14|||Glikson et al. (1996), Howard et al. (2011). Eastern Mann Ranges (Fregon Domain) and Pottoyu Hills (Mulga Park Domain). Similar textures to the Type-C mafic dykes of Glikson et al. (1995) which have a poorly constrained Sm-Nd age of 1000 Ma.|1,000 Ma.|||Intrudes the Angatja and Pottoyu Suites.|Olivine dolerite dykes, generally trending NNE; have undergone metamorphic recrystallisation; local olivine gabbro bodies.|12-JUL-16
74604|Kullal Dyke Suite|69655|6|Mentioned|p6|||||||||
74604|Kullal Dyke Suite|69729|5|Briefly described|p68, p74 Fig.8, p84, p86|||Composition and Nd-isotopes contrasted with Alcurra Dolerite. Trace element plot. Appears as Kullal dyke suite on p86. This age (Glikson et al., 1996) is described as "poorly constrained".|c.1000 Ma(Sm-Nd mineral isochron age).|||Crocss-cuts Alcurra Dolerite.|Fine-grained olivine and plagioclase porphyritic dolerite dykes.|
74604|Kullal Dyke Suite|70338|5|Briefly described|Map legend.|Neoproterozoic|Mesoproterozoic||c.1000 Ma.||||Dolerite, fine-grained; olivine and plagioclase, typically porphyritic; meta-dolerite, typically porphyritic, granoblastic.|
74604|Kullal Dyke Suite|70634|4|Described|100k_interpgeol_lut.csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age is of an inherited component and thus only constrains maximum age of dolerite dyke sample age (194759.1.pdf)|1000 Ma (Inferred) 1372 Ma +/- 14 Ma (SHRIMP)||||Fine-grained olivine--plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed.|
74604|Kullal Dyke Suite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). Most common in the Hinckley Range and Michael Hills areas of BELL ROCK 1:100 000 sheet; typically forms NE-trending, narrow (0.5-5 m wide) dykes of fine grained olivine- and plagioclase-phyric dolerite (Howard et al., 2011). Sample GSWA 194759 (porphyritic dolerite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) maximum igneous crystallisation age of 1372+\-14 Ma. See 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1000 Ma (inferred)|||Intrudes into Warakurna Supersuite. Intruded by Gairdner Dolerite.|Fine-grained olivine-plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed|
74604|Kullal Dyke Suite|70839|5|Briefly described|p327|Proterozoic|Proterozoic|Geological province: Musgrave Province. Mafic intrusives with poorly constrained Sm-Nd mineral isochron date of c. 1 Ga (Glikson et al., 1996).||||||
74604|Kullal Dyke Suite|71088|5|Briefly described|p4||||c. 1000 Ma||||Mafic rocks.|
74604|Kullal Dyke Suite|71170|5|Briefly described|p6|||||||||
74604|Kullal Dyke Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Most common in Hinckley Range and Michael Hills areas of BELL ROCK 1:100 000 sheet, typically forms NE-trending, narrow (0.5-5 m wide) dykes of fine-grained olivine- and plagioclase-phyric dolerite (Howard et al., 2011). Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). Sample GSWA 194759 (porphyritic dolerite) yielded a concordia age of 1372+\-14 Ma, interpreted as age of an iherited component in the dyke magma, and therefore provides a maximum age of igneous crystallisation age of the dolerite dyke. See 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1000 Ma (Inferred)||||Fine-grained olivine--plagioclase dolerite and metadolerite; typically porphyritic; granoblastic where metamorphosed|
74604|Kullal Dyke Suite|71321|5|Briefly described|p4,11,14,22-23,50,52-54,59,62,64|Stenian|Stenian|Geological province: Musgrave Province. [Also referred to as Kullal Dolerite on p1]. Comprises part of basement to the Musgrave Province. Occurs as high-Mg suite of olivine dolerites generally forming thin NNE to ENE trending dykes, typically less than 10m but up to 20m wide. See p52-54 for detail geochemical breakdown and anaylsis.|||||Dolerite; fine-grained; olivine and plagioclase, typically porphyitic; meta-dolerite, typically porphyritic, granoblastic.|
74604|Kullal Dyke Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|||||Dolerite dyke.|
79540|Kullal Dykes|69003|6|Mentioned|p4|||Paterson Orogen.||||||
79540|Kullal Dykes|70084|6|Mentioned|p220|||West Musgrave Province. Coeval with the Giles Event and emplacement of the Bentley Supegroup.||||||
80187|Kullal Suite|68077|6|Mentioned|p31|||Age is an imprecise Sm-Nd mineral isochron (Glikson et al., 1996).|c.1000 Ma.||||Includes a plagioclase- and olivine-phyric dolerite (dyke).|
80187|Kullal Suite|73058|6|Mentioned|p770|Tonian|Stenian|Porphyritic dolerite dyke contains an inherited 1372+/-14 Ma zircon population.|c. 1000 Ma Sm-Nd mineral isochron||||Includes a fine-grained plagioclase and olivine porphyritic dolerite dyke.|
77413|Kullal dykes|65135|5|Briefly described|p17|Stenian|Stenian|Informal name. Fine-grained olivine and plagioclase porphyritic dolerites. Most common in the Michael Hills and Hinckley Range regions. Typically northeast trending. Cross-cuts igneous layering of the Giles intrusions and are cut by the ~825 Ma Gairdner dykes. Poorly constrained ~1000 Ma age from Sm-Nd mineral isochron.||||||
77413|Kullal dykes|65693|5|Briefly described|p4, p12.|Neoproterozoic|Mesoproterozoic|Term used throughout the article, presumably as shorthand for the formally-named Kullal Dyke Suite. Probably generated from similar magma source to Alcurra Dolerite. Age poorly constrained but either similar to, or younger than Alcurra suite.|~1000 Ma|||||30-OCT-12
69693|Kunagunarinna Formation|61253|5|Briefly described|p51|Archean|Archean|Place name is Kunagunarrina - this name may be misspelt?  Of the Sulphur Springs Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
69693|Kunagunarinna Formation|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of Sulphur Springs Group (Pilbara Supergroup).||||||07-FEB-11
69693|Kunagunarinna Formation|66745|4|Described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Deepening of depositional basin. [misspelling of Kunagunarrina]||Unit in Sulphur Springs Group.||Overlies Leilira Formation. Is overlain by Kangaroo Caves Formation.|Basalt, komatiitic basalt.|23-MAY-16
69693|Kunagunarinna Formation|67201|5|Briefly described|p7 Fig.4, p12 Tb.1, p24|||In northern Pilbara Craton, East Pilbara Terrane. Appears [correctly spelt] as Kunagunarrina Formation on p24.||Sulphur Springs Group||||24-NOV-16
69693|Kunagunarinna Formation|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Sulphur Springs Group.||Overlies Leilira Formation. Is overlain by Kangaroo Caves Formation.|Komatiitic basalt.|
69693|Kunagunarinna Formation|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.||||
69693|Kunagunarinna Formation|68035|5|Briefly described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane, Pilbara Craton.||Of Sulphur Springs Group.||Overlies Leilira Formation. Overlain by Kangaroo Caves Formation.|Komatiitic basalt, basalt.|
69693|Kunagunarinna Formation|68280|5|Briefly described|p4|||||Sulphur Springs Group||Overlies Leilira Formation, overlain by Kangaroo Caves Formation|Basalt and komatiitic basalt.|
69693|Kunagunarinna Formation|68284|5|Briefly described|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Sulphur Springs Group.||Overlies Leilira Formation. Is overlain by Kangaroo Caves Formation.||
69693|Kunagunarinna Formation|69301|5|Briefly described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane.||Sulphur Springs Group|||Basalt, komatiitic basalt.|
69693|Kunagunarinna Formation|69616|5|Briefly described|p161|Archean|Archean|[Mis-spelling of Kunagunarrina].||Unit in Sulphur Springs Group.||Overlies Leilira Formation. Is overlain by Kangaroo Caves Formation.||
69693|Kunagunarinna Formation|70022|6|Mentioned|p115|||East Pilbara Terrane.||Sulphur Springs Group.||||
69693|Kunagunarinna Formation|70775|5|Briefly described|p12, p24-p25|||East Pilbara.||Sulphur Springs Group||Overlies the Leilira Formation. Overlain by the Kangaroo Caves Formation.||
69693|Kunagunarinna Formation|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Overlain by Kangaroo Caves Formation. Underlain by Leilira Formation.||
69693|Kunagunarinna Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Uppermost unit of Sulphur Springs Group. Overlain by Kangaroo Caves Formation. Underlain by Leilira Formation.||
69693|Kunagunarinna Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Sulphur Springs Group.||Overlain by Cangaroo Caves Formation. Underlain by Leilira Formation.||
69693|Kunagunarinna Formation|72668|5|Briefly described|p4|||East Pilbara Terrane. See also Kunagunarrina Formation p5, p6.||Sulphur Springs Group||Overlies the Leilira Formation. Overlain by the Kangaroo Caves Formation.||13-JAN-22
69693|Kunagunarinna Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Sulphur Springs Group.||Overlies Leilira Formation. Is overlain by Kangaroo Caves Formation.||
76765|Kunamanara Group|64722|5|Briefly described|p17|Stenian|Stenian|Smithies et al. (2008) define this group as an older component of the old Tollu Group, synchronous with intrusion of the Giles Complex, and re-define the Tollu Group. Stenian age therefore inferred.||||||
83383|Kundana Formation|73391|6|Mentioned|p179|||Forman (1937). Later (1953) included with the Kurrrawang Formation. Krapez etal. (2008) proposed it be named the Navajo Supersequence, and correlated it with the Merougil Formation at Kambalda.|||||A 700m thick conglomerate.|
28656|Kundana Series|42892|6|Mentioned|Table 4|||||||||
28656|Kundana Series|73391|6|Mentioned|p233-234, Appendices.|||Talbot (1934). These rocks were later (Feldmann, 1936; Formann, 1937) interpreted as belonging to the Kurrawang Series. Regional stratigraphic correlation chart of previous workers.|||||Grit, sandstone, shale, basal conglomerate.|
80037|Kunganna Formation|67130|6|Mentioned|p24, p31|||[Misspelling of Kungarra Formation].||Turee Creek Group||||20-SEP-17
34927|Kuniandi Formation|22901|6|Mentioned|76 fig 2|||||||||
41578|Kuniandi group|22496|6|Mentioned|p10|||Informal name - Kuniandi Group.||||||12-AUG-04
77419|Kunmanarra Group|65907|5|Briefly described|p6.||||c.1120-1078 Ma.||||Basal conglomerates and sandstones, basalt.|01-MAY-15
77693|Kunnunurra Member|68298|5|Briefly described|p216|||Bonaparte Basin. Limestone horizon||Cockatoo Formation||||
26675|Kununurra Member|32664|6|Mentioned|Map legend|Late Devonian|Late Devonian|Briefly described in notes||||||
26675|Kununurra Member|32865|6|Mentioned|p468|||Frasnian||||||
26675|Kununurra Member|36890|4|Described|p376|||||||||
26675|Kununurra Member|42994|6|Mentioned|p50|||of Cockatoo Formation||||||
26675|Kununurra Member|45038|2|Defined|p.17,22||Late Devonian|U.Dev.||||||
26675|Kununurra Member|45039|6|Mentioned|p7|||Upper Devonian. See also PP8,18,148.||||||
26675|Kununurra Member|45040|14|Not recorded|p5, fig.2||Late Devonian|(Upper Devonian). Pt. Cockatoo Formation.||||||
26675|Kununurra Member|45050|6|Mentioned|p45|||See also P57||||||
26675|Kununurra Member|45063|6|Mentioned|p6|||See also P12, 23 & Fig. 3. Frasnian||||||
26675|Kununurra Member|48886|14|Not recorded|Map||Late Devonian|Upper Devonian. Defn. on Tech.File D/52-14.||||||
39988|Kuranna Granitoid Complex|24184|5|Briefly described|p717|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3.45Ga||||||07-NOV-08
83149|Kurnalpi Group|72491|6|Mentioned|p5 Fig.4|||Kurnalpi Terrane, Yilgarn Craton.||||||
77095|Kurnalpi Sequence|63980|4|Described|p57, pp62-63.|Archean|Archean|Kurnalpi Terrane. In this study, refers to Association 2 of Hallberg (1985): andesitic complexes of lavas and conglomerates older than 2.7 Ga. Poor outcrops of chlorite-rich schists and metamorphosed shales. Similar to intra-oceanic arc volcanic centres.||||Overlies Laverton Sequence. Is overlain by Minerie Sequence.||
77095|Kurnalpi Sequence|64633|5|Briefly described|p4 Fig.3. |||Kurnalpi Terrane.|c.2717 - 2715 Ma.|||Is overlain by Minerie Sequence.||
77095|Kurnalpi Sequence|66880|4|Described|p9, pp26-27. |Archean|Archean|Term used in this study for the dominant association of andesitic volcanic rocks and feldspathic sedimentary rocks in the Kurnalpi Terrane. Interpreted to underlie Gindalbie Sequence. Records emergent arc-related volcanism.|c.2715-2704 Ma.||Includes Minerie Sequence.||Calc-alkalic andesite and dacite lavas and associated volcaniclastics; subordinate felsic dacites and rhyolites; intruded and overlain by extensive basalt-dolerite-gabbro-komatiitic sequence with minor volcaniclastic and epiclastic sedimentary rocks.|
77095|Kurnalpi Sequence|66937|6|Mentioned|p167 Fig.10.|Archean|Archean|||||||
77095|Kurnalpi Sequence|67198|5|Briefly described|p5 Fig.2, p7, p46-48|Neoarchean|Neoarchean|Kurnalpi Terrane. Calc-alkalic andesite-dominated sequence. Ages derived from volcaniclastic turbiditic rocks and inferred to be depositional ages. Another age that is provided is  2704 +/- 4 Ma (Kositcin et al, 2008 - SHRIMP)|2715 +/- 5 Ma |||Unconformably overlies Laverton Sequence. Is overlain conformably by the Minerie Sequence.|Andesitic lavas and andesitic volcaniclastic sedimentary rocks that grade up into quartz bearing sandy turbiditic rocks and conglomerate with clasts of dacite and andesite. Locally the turbiditic rocks grade up into magnetic shales.|11-SEP-17
77095|Kurnalpi Sequence|68107|6|Mentioned|p618, p619 Fig.8|Neoarchean|Neoarchean|Kurnalpi Terrane.|ca. 2715-2704 Ma|||||
77095|Kurnalpi Sequence|68186|5|Briefly described|p5|Archean|Archean|Eastern Kurnalpi Terrane, Eastern Goldfields Superterrane. Represents inter-arc complexes.|2715-2704 Ma.||||Calc-alkaline, andesite-dominated complexes.|
77095|Kurnalpi Sequence|69404|6|Mentioned|p4 Fig.4|Neoarchean|Neoarchean|Kurnalpi Terrane.|c. 2700 Ma|||||
77095|Kurnalpi Sequence|69586|5|Briefly described|p1|||Eastern Kurnalpi Terrane. Interpreted as a series of intra-arc complexes.|2715-2704 Ma.||||Calc-alkaline andesite-dominated complexes.|
77095|Kurnalpi Sequence|70020|5|Briefly described|p121|Neoarchean|Neoarchean|Geological province: Kurnalpi Terrane, Yilgarn Craton.||||Overlain by Minerie Sequence.|Basalt, dolerite/gabbro intrusions; komatiitie and komatiitic basalt, intermediate volcanic rocks.|
77095|Kurnalpi Sequence|70087|5|Briefly described|p214-215, 222|Archean|Archean|Base of Kurnalpi Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. At least 3.2 km thick.|2715 +/- 5 Ma to 2702 +/- 5 Ma.|||Is overlain conformably by (or tectonically interleaved with) the Minerie Sequence.|Greenstone successions; andesitic to felsic volcanic rocks and coarse volcaniclastic sediment with subordinate lava flows. Upper prehnite-pumpellyite to lower greenschist facies.|
77095|Kurnalpi Sequence|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kurnalpi Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.||||||
77095|Kurnalpi Sequence|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlain by the Minerie Sequence.||
77095|Kurnalpi Sequence|71308|6|Mentioned|p711 Fig.2|||Kurnalpi Terrane.||||||
77095|Kurnalpi Sequence|71309|6|Mentioned|p740 Fig.3|||||||||
77095|Kurnalpi Sequence|72485|6|Mentioned|p3 Fig.2|||||||||
33907|Kurrana Downs Granitoid Complex|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2900 Ma.||||||27-JAN-09
22147|Kurrana Granite|23936|6|Mentioned|p19|||Geological Province: Pilbara Craton.||||||
22147|Kurrana Granite|24188|6|Mentioned|p789, Fig.2a|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
74725|Kurrana Granitic Complex|64580|4|Described|map legend||Mesoarchean|Biotite metamonzogranite and gneissic metagranodiorite with greenstone xenoliths, foliated to gneissic biotite metamonzogranite and metasyenogranite, and muscovite-bearing monzogranite.||||||15-DEC-08
74725|Kurrana Granitic Complex|65825|5|Briefly described|p1, p6, p12, pp31-32.|Archean|Archean|Appendix 2 correlates this unit with the Split Rock Supersuite and the Mount Billroth Supersuite in the GSWA database. Along the contact with this unit, the Coondamar Formation experienced amphibolite facies metamorphism.|||Includes Golden Eagle Orthogneiss and Bonney Downs Granite.|||
37861|Kurrana Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: c.3300Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
37861|Kurrana Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
37861|Kurrana Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p146 Tb.2-21|||See also p153 Fig.2-140. |||Includes Bonney Downs Granite.||Syenogranite, foliated and schistose monzogranite, migmatite.|
37861|Kurrana Granitoid Complex|44152|6|Mentioned|p166|||||||||
37861|Kurrana Granitoid Complex|50287|5|Briefly described|Map Legend|Archean|Archean|Of Kurrana Granitoid Complex. Geological Province: Kurrana Terrane, Pilbara Craton.||||||07-NOV-08
37861|Kurrana Granitoid Complex|61264|5|Briefly described|p63 Fig. 1|Archean|Archean|Age: 3200-2840Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
37861|Kurrana Granitoid Complex|64653|5|Briefly described|Map Legend|Archaean|Archaean|Includes Bonney Downs Granite. Age: 3199-3178Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
37861|Kurrana Granitoid Complex|65828|6|Mentioned|Map legend|Archean|Archean|Kurrana Terrane, Pilbara Craton.|||Includes Golden Eagle Orthogneiss and Bonney Downs Granite.|||
37861|Kurrana Granitoid Complex|69167|6|Mentioned|178012.1.pdf|||(Structural?)||||||
39720|Kurrana Granitoid complex|24188|6|Mentioned|p788 Fig.1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
78796|Kurrana granitic complex|63854|6|Mentioned|p229 Fig.2|||Kurrana Terrane, Pilbara Craton.||||||
39746|Kurrana granitoid complex|24193|5|Briefly described|p874 Fig.1, p878 Tb.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
67865|Kurrawang Formation, lower|60076|5|Briefly described|p47 App. 1|||Informal - see Kurrawang Formation.  Conglomerate, sandy conglomerate and pebbly sandstone; banded-iron formation pebble horizon.||||||
67866|Kurrawang Formation, upper|60076|5|Briefly described|p48 App. 1|||Informal - see Kurrawang Formation.  Sandstone and pebbly sandstone.||||||
83384|Kurrawang Sandstone|73391|5|Briefly described|p88, 96, 98, 101, 194, 244-245|||See also Appendices. One of four ""major subdivisions"" of Kurrawang Formation, but like the others is not given the rank of Member. Presented as Kurrawang sandstone on p98, 244. Lithology detailed; photographs, photomicrographs. There is also, confusingly, an un-named sandstone unit in this quartet. ~290m thick.||Uppermost Kurrawang Formation.|||Thickly-bedded, trough cross-bedded quartz sandstone with polymictic pebble lags and rare siltstone interbeds, and a thin unit of plane-bedded sandstone and siltstone.|
77544|Kurrawang Sequence|63981|5|Briefly described|p91, p93 Fig.3, |Archean|Archean|One of four unconformity-bounded second-order sequences recognised in the Kalgoorlie Terrane. There is a formally-named unit, the Kurrawang Formation.|||||Turbidite sequences.|
77544|Kurrawang Sequence|65260|6|Mentioned|p6 Tb.1|Neoarchean||2655 Ma.||||||
77544|Kurrawang Sequence|66880|5|Briefly described|p7. |Archean|Archean|Current formal name is Kurrawang Formation. Part of the uppermost of three lithostratigraphic divisions in the Kambalda Domain. Submarine-fan deposits.|Max. age 2658 +/- 3 Ma.|||||
77544|Kurrawang Sequence|67198|5|Briefly described|p81-83|||||||Unconformably overlies Kalgoorlie Sequence.|An upward-fining turbidite succession of conglomerate, sandstone and mudstone.|11-SEP-17
77544|Kurrawang Sequence|68109|6|Mentioned|p660|Neoarchean|Neoarchean||> 2660 Ma|||Unconformably overlies the Kambalda and Kalgoorlie Sequences.||
77544|Kurrawang Sequence|73391|6|Mentioned|Appendices.|||Krapez et al. (2000). Regional stratigraphic correlation chart of other workers.||||||
34371|Kurrawang Supersequence|22682|5|Briefly described|p14|||Overlies Black Flag Supersequence with a fault or unconformity||||||
34371|Kurrawang Supersequence|66936|5|Briefly described|pp136-137, pp141-144. |Archean|Archean|Kalgoorlie Terrane. At least 1750 m thick. The lower part is interpreted to be fill of a submarine canyon.||||Unconformably overlies Kalgoorlie Sequence.|Conglomerate, minor sandstone; overlain by sandstone succession; minor black shale.|
34371|Kurrawang Supersequence|66937|6|Mentioned|p155. |Archean|Archean|Kalgoorlie Terrane.||||||
34371|Kurrawang Supersequence|66938|5|Briefly described|p186. |Archean|Archean|Sediment derived from a fluvial system sourced outside the Eastern Goldfields Superterrane.||||||
34371|Kurrawang Supersequence|73391|6|Mentioned|Appendices.|||Krapez and Pickard (2010). Regional stratigraphic correlation chart of other workers.||||||
38640|Kurrawong Formation|23786|5|Briefly described|p5|||Max. thickness: 1800m.  Geological Province: Eastern Goldfields Province.||||||
75508|Kurriyippi Formation|64630|5|Briefly described|p31 Fig.2, p37|Sakmarian|Sakmarian|N.B. Misspelling of Kuriyippi. Province: Bonaparte Basin. Part of the Kulshill Group, underlies the Treachery Shale, overlies the Wadeye Group. Palynology age: P. confluens. Inferred glacial influence.||||||18-JAN-10
75508|Kurriyippi Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Bonaparte Basin.||||Overlain by the Treachery Shale.||
25138|Kurruwang beds|31038|6|Mentioned|p404|||Archaean. See also P407, 408||||||
27454|Kuruna Siltstone|23570|5|Briefly described|p123|||See also Maddina Formation.   Geological Province: Pilbara Craton||||||
27454|Kuruna Siltstone|23585|5|Briefly described|p14 Fig 5|Archean|Archean|Of Fortescue Group. Overlying unit Pearana Basalt. Underlying unit Nymerina Basalt. Hamersley Basin.||||||07-NOV-08
27454|Kuruna Siltstone|23594|6|Mentioned|p17|||||||||
27454|Kuruna Siltstone|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Fortescue Group.  Age: c.2.76-2.69Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
27454|Kuruna Siltstone|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.76-2.69 Ga. Geological Province: Pilbara Craton. Parent: Fortescue Group. Overlying Unit: Maddina Basalt. Underlying Unit: Nymerina Basalt.||||||07-NOV-08
27454|Kuruna Siltstone|24353|4|Described|p26|Archean|Archean|Overlying Unit: Maddina Basalt. Underlying Unit: Nymerina Basalt. Parent: Maddina Formation. Geological Province: Pilbara Craton||||||07-NOV-08
27454|Kuruna Siltstone|31307|6|Mentioned|p80|||Stratigraphy||||||
27454|Kuruna Siltstone|35641|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27454|Kuruna Siltstone|36551|6|Mentioned|Table 23|||||||||
27454|Kuruna Siltstone|37460|3|Fully described|Table 3.I|||||||||
27454|Kuruna Siltstone|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27454|Kuruna Siltstone|39426|4|Described|p11|||||||||
27454|Kuruna Siltstone|39444|4|Described|p36|||||||||
27454|Kuruna Siltstone|39697|4|Described|p122|||||||||
27454|Kuruna Siltstone|39837|6|Mentioned|Table 1|||||||||
27454|Kuruna Siltstone|40369|6|Mentioned|p15|||See also Table 1||||||
27454|Kuruna Siltstone|40904|6|Mentioned|Table 1|||||||||
27454|Kuruna Siltstone|41357|6|Mentioned|Fig.2|||||||||
27454|Kuruna Siltstone|41635|6|Mentioned|Table 2|||||||||
27454|Kuruna Siltstone|41669|6|Mentioned|p25|||||||||
27454|Kuruna Siltstone|42352|5|Briefly described|p5|||||||||
27454|Kuruna Siltstone|42785|6|Mentioned|Fig.6 P272|||||||||
27454|Kuruna Siltstone|43055|6|Mentioned|p15|||||||||
27454|Kuruna Siltstone|43595|6|Mentioned|Table 2-29,p219|||Included within Pillingini Tuff (maybe superseded)||||||
27454|Kuruna Siltstone|43698|6|Mentioned|p26|||||||||
27454|Kuruna Siltstone|44152|6|Mentioned|p177|||Not recognised in Gregory Range area.||||||
27454|Kuruna Siltstone|44443|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
27454|Kuruna Siltstone|46319|4|Described|p14|Proterozoic|Paleoproterozoic|Of Fortescue Group. Maximum thickness: 20m.||||||28-MAY-14
27454|Kuruna Siltstone|50189|5|Briefly described|p23|Archean|Archean|Superseded by the Kuruna Member. Formerly occured between what were previously the Nymerina Basalt and the Maddina Basalt - all now grouped into the Maddina Formation.||||||07-NOV-08
27454|Kuruna Siltstone|50544|6|Mentioned|p44 Fig. 8|Archean|Archean|Of Macleod and de la Hunty (1966); Hickman et al (1983).  Superseded by Kuruna Member.||||||07-NOV-08
27454|Kuruna Siltstone|60429|5|Briefly described|p20 Fig. 5, p21, p23|Archean|Archean|Incorporated as Kuruna Member into Maddina Formation - due to its discontinuous outcropping which, when absent, made it impossible to distinguish Maddina Basalt from the underlying Nymerina Basalt - all three forming the new Maddina Formation.||||||07-FEB-11
27454|Kuruna Siltstone|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
27454|Kuruna Siltstone|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Geological province: northen Pilbara Craton. Sandstone and siltstone; shale; ooidal sediments; pisolitic tuff and banded siliceous limestone.||||||07-FEB-11
27454|Kuruna Siltstone|65825|6|Mentioned|p22.|Archean|Archean|Superseded name; now included in Maddina Formation.||||||
27454|Kuruna Siltstone|65827|6|Mentioned|Fig.6 p33, p39|Neoarchean|Neoarchean|MacLeod and de la Hunty (1966). Former name of Kuruna Member in Nullagine 1:250 000 map. Shown as equivalent to Mount Jope Supersequence (2).
||||||
27454|Kuruna Siltstone|67229|6|Mentioned|p3 Fig.2|||Of Hickman (1983) after MacLeod and de la Hunty (1965). Hickman divided the Pillingini Tuff of Kriewaldt and Ryan (1967) into three Formations including this unit.||||||
27454|Kuruna Siltstone|69299|5|Briefly described|p4, p19|||Replaced by Kuruna Member. Was intervening sedimentary unit between former Nymerina Basalt and Maddina Basalt (Hickman 1983). Thorne and Tyler (1997a) redefined Maddina Basalt to include all rocks previously separately assigned to the Nymerina Basalt, Kuruna Siltstone, and Maddina Basalt. Maddina Basalt was later renamed Maddina Formation. Sometimes presented as 'Kuruna Siltstone' in text.||||||
78670|Kuryippi Formation|13234|6|Mentioned|p250 Fig.2|Late Carboniferous|Late Carboniferous|Mis-spelt: see Kuriyippi Formation (p256). Contains biodegraded oil. Proven reservoir.||||||27-OCT-14
78356|Kynea Tonalite|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
78356|Kynea Tonalite|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|||Bunnawarra Suite|||Tonalite.|
78356|Kynea Tonalite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Bunnawarra Suite.||||
78356|Kynea Tonalite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2950 Ma.|Bunnawarra Suite.|||Migmatitic tonalite (to granodiorite) gneiss with metamonzogranitic leucosomes.|
78356|Kynea Tonalite|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Mesoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv. Numerous additional lithologies are discussed.|2950 +/ 30 Ma (isotopic)|Bunnawarra Suite|||Migmatitic tonalite (to granodiorite) gneiss with metamonzogranitic leucosomes|
78356|Kynea Tonalite|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeol_lut.csv.|2950+\-30 Ma|Unit of Bunnawarra Suite.|||Migmatitic tonalite (to granodiorite) gneiss with metamonzogranitic leucosomes|
78356|Kynea Tonalite|73023|5|Briefly described|p2-3|Mesoarchaean|Mesoarchaean|Constitutes the core of the Yalgoo Dome in the western Murchison Domain, Youanmi Terrane, Yilgarn Craton.|2970-2930 Ma.|||Is surrounded by Goonetarra Granodiorite. Is intruded by Bald Rock Supersuite.|Migmatitic tonalite-trondhjemite-granodiorites.|
72829|Labouchere Formation, lower|49896|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Informal - see Labouchere Formation. Contains a quartzite marker at base.||||||07-NOV-08
32584|Lady Mary Formation|45543|6|Mentioned|p.101-106|||Table 2.||||||
73862|Lagoon Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Cleaverville Group. Thick pillow basalt, rhyolite lava, a few chemical sediments; top section comprises the informally named Lagoon Pillow Basalt - part of the main formation. Geological Province: Pilbara Block.||||||07-NOV-08
73862|Lagoon Formation|68574|6|Mentioned|p3-5|||Kiyokawa and Taira (1998), for rocks previously part of the Regal Formation (Ryan, 1965). The name is invalid (reasons given).||||||
73863|Lagoon Pillow Basalt|24391|4|Described|p8-4 Fig.2|Archean|Archean|Top of Lagoon Formation within the Cleaverville Group. Informal name. Thick pillow basalt, rhyolite lava, a few chemical sediments; probably part of the underlying Lagoon Formation. Overlain by Dixon Island Formation. Geological Province: Pilbara Block.||||||07-NOV-08
73863|Lagoon Pillow Basalt|68574|6|Mentioned|p4-5|||Kiyokawa and Taira (1998), for rocks previously part of the Regal Formation (Ryan, 1965). The name is invalid (reasons given). These rocks are included in the Regal Formation (Ryan and Kriewaldt, 1964).||||||
70439|Laguna Green granite|61273|6|Mentioned|p87|||Not intended as a formal stratigraphic name. Commercial name for dimension stone quarried near Jerramungup.||||||
81731|Lake Douglas Conglomerate|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma; Yilgarn Craton events (4000 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2657+\-7 Ma; 2640 Ma|Unit of Kurrawang Formation.|||Conglomerate, sandy conglomerate, and pebbly sandstone; metamorphosed|
79539|Lake MacKay Quartzite|69003|5|Briefly described|p5, p31|Paleoproterozoic|Paleoproterozoic|West Arunta Orogen and Amadeus Basin. May correlate with the Reynolds Range Group in NT.|< 1750 +/- 19 Ma (maximum deposition age).|||Overlies Carrington Suite.|Deformed and strongly recrystallised quartzite.|
79539|Lake MacKay Quartzite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.||||Overlies Lander Rock Formation and Carrington Suite.|Interbedded quartzite and quartz-mica schist.|
83225|Lake McKay Quartzite|73445|5|Briefly described|p7, 10|||West Arunta Orogen.|1750 +/- 19 Ma (MDA: Kirkland et al., 2009).|||Overlies Lander Rock Formation. Is overlain unconformably by Munyu Sandstone.||
25146|Lake Nyanga Shale""|32552|6|Mentioned|p39|||Refers Jackson (1966)||||||
83930|Lake Seabrook Granite|70281|6|Mentioned|p454, 456-457, 478 Appendix 2|||Southern Cross terrane, Yilgarn Craton. Is associated with a 6 km-long zone of low-grade tungsten skarn. Rb-Sr isotope data tabulated. Is presented informally as Lake Seabrook granite or Lake Seabrook pluton in the text, but appears in Appendix 2 as Nevoria and Lake Seabrook Granites.|2656 +/- 3 Ma (Qiu et al., 1999).|||||
27458|Lake Willson Beds|29813|4|Described|Table 2|||||||||
27458|Lake Willson Beds|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27458|Lake Willson Beds|38243|6|Mentioned|p354|||||||||
27458|Lake Willson Beds|38988|6|Mentioned|p16|||||||||
27458|Lake Willson Beds|45140|2|Defined|p40, p42-43, p66, p74, Appx.p21-22|Proterozoic|Proterozoic|Blake et al. (1977). Named after Lake Willson. Mapped as Gardiner Beds by Casey and Wells (1964). Crops out mainly as flat-lying chert, commonly stromatolitic. The reference area is a NW-dipping sequence 20km S of Sturt Creek homestead, on the track to Balgo, at 19deg 19'S, 128deg 12'E. At least 150m thick. See also Lake Wilson Beds (p13).||||Tentatively correlated with Talbot Well Formation. May overlie Gardiner Sandstone (or equivalent). Inferred to underlie the Pindar Beds conformably, and the Chuall Beds unconformably.|Interbedded chert, commonly stromatolitic, and cross-bedded, medium- to coarse-grained sublithic arenite; also shale and siltstone.|
27458|Lake Willson Beds|46864|6|Mentioned|p38|||See also Fig.3.||||||
73567|Lakeside Member|63454|5|Briefly described|p71 Tb. 2|||Abbreviated version of Lakeside Limestone Member - used interchangeably in this article.||||||
82960|Lakewood Dacite|73238|5|Briefly described|p21|||Kanowna district, Eastern Goldfields Terrane.|2672 +/- 6 Ma (Tripp, 2013).|||||
79228|Lakewood Dolerite Suite|70794|5|Briefly described|2_5m_interpdykel15_lut.csv|Proterozoic|Proterozoic|Mainly northwest-trending dykes.|2500-541 Ma inferred.||||Dolerite.|
79228|Lakewood Dolerite Suite|70802|5|Briefly described|2_5m_interpdykel15_lut.csv|Proterozoic|Proterozoic|Geological province: Albany-Fraser Orogen. Events: Western Australian events (4000-0.01 Ma).|2500-510 Ma (inferred)||||Dolerite; mainly northwest-trending dykes|
79228|Lakewood Dolerite Suite|70826|6|Mentioned|p14 tbl 5|||Yilgarn Craton. 2500-541 Ma age range [not useful].||||||
79228|Lakewood Dolerite Suite|71270|4|Described|GEOL_LUT_CSV files|Proterozoic|Proterozoic|Events: Western Australian events (4000 - 0.01 Ma). See 100k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|2500-541 Ma (inferred)||Includes Parkeston Dolerite.||Dolerite; mainly northwest-trending dykes|
83385|Lakewood dacite|73391|5|Briefly described|p194, 196, 244, 246, 304, 308, 315, 419|||Kambalda Domain, Kalgoorlie Terrane. Often referred to as Lakewood dacites; Lakewood Dacites on p308.|2672 +/- 6 Ma U-Pb SHRIMP|Lower Black Flag Formation.||Overlies Talbot formation. Is overlain unconformably by Gidji Lake formation. Correlated with Gibson-Honman formation.||01-JUL-22
78673|Lalla Rookh Sequence|60112|6|Mentioned|p109 Fig.2. |||||Unit in De Grey Group.||||
35559|Lalla Rookh sandstone|23255|6|Mentioned|Fig.3|||Misspelt.||||||
40158|Lalla Rookh sediments|24621|5|Briefly described|p75|Archean|Archean|Informal name.  Age: ~2950Ma.||||||07-NOV-08
25149|Lamboo Complex gneisses|30097|6|Mentioned|Table 24|||||||||
77853|Lamil Formation|60470|6|Mentioned|p9|||[probable misspelling of Lamil Group]. Said to be overlain by Paterson Formation.||||||
69967|Lamil group|50228|5|Briefly described|p477, p482|Neoproterozoic|Neoproterozoic|Informal - see Lamil Group. May be a correlative of the c.690-605Ma Supersequence 2 of the Centralian Basin? Geological Province: Yeneena Basin.||||||
72629|Laminaria/Elang Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Jurassic|Informal compound term to include both Laminaria and Elang Formations. Age: ~163-~157Ma. Geological Province:  Northern Bonaparte Basin.||||||
77545|Lancefield Sequence|66880|6|Mentioned|p28.|Archean|Archean|There is a formally-named unit, the Lancefield Conglomerate. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank.|2684 +/- 5 Ma.|||||
38658|Lancefield conglomerate|23786|5|Briefly described|p27|||Informal name - see Lancefield Conglomerate.  Geological Province: Yilgarn Craton.||||||
74157|Landrigan Formation|63762|5|Briefly described|p19|||Correlate of Walsh Formation. See also Landrigan Tillite.||||||07-FEB-11
74157|Landrigan Formation|64104|6|Mentioned|p70 Fig.7.|Neoproterozoic|Neoproterozoic|The author proposes this name replace Landrigan Tillite "to distinguish stratigraphic terms from genetic interpretation".||||||
74157|Landrigan Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Mount Ramsay area, West Kimberley. ||Of the Kuniandi Group.||Overlain by the Stein Formation.||
74157|Landrigan Formation|67620|5|Briefly described|p5|Cryogenian|Cryogenian|Mount Ramsay area, Kimberley region.||Kuniandi Group.||Is overlain by Stein Formation.||
74157|Landrigan Formation|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Mount Ramsay area, Kimberley region.||Kuniandi Group.||||
74157|Landrigan Formation|68244|4|Described|p659-660,662-666,669-671|Neoproterozoic|Neoproterozoic|Louisa Basin, Kimberley region. Thickness at type section: 350m. Glaciogenic unit deposited during of Landrigan Glaciation. See p665-666 for detailed lithology and depositional environment. Cap dolomicrite likely deposited in a low energy, deep-water environment. Correlative to Walsh Fm (Mount House Gp), and Mountain Valley Fm, Frank River Sst and Fargoo Fm (Duerdin Gp). Underlain by Kimberley Group, Bow River Granite, basement. Also unconformably overlies the Carson Volcanics.||Unit of Kuniandi Group.||Lowermost unit of Kuniandi Gp. Overlain by Stein Fm.|Intercalated sandstone, siltstone, diamictite and conglomerate and is overlain by a thin unit (c. 9 m thick) of sandy to thinly laminated dolomite.|21-JUN-19
74157|Landrigan Formation|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
74157|Landrigan Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
38972|Landrigan tillite|23806|6|Mentioned|p1121|Neoproterozoic|Neoproterozoic|Misspelt - see Landrigan Tillite.||||||
81604|Langenbeck Supersuite|72251|6|Mentioned|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton. Poorly labelled diagram.||||||23-DEC-19
28667|Langey Shale""|22776|6|Mentioned|p21|||Equivalent to Jarlemai Siltstone.||||||
28667|Langey Shale""|45158|6|Mentioned|p15|||||||||
33012|Lansdowne Formation|44366|14|Not recorded|p.13, Table 2|||||||||
72579|Larranganni beds|65074|4|Described|p351, p360, p361 Tb. 4-14, p362|Mesozoic|Mesozoic|Of North/Centre Birrindudu Basin. Possibly Triassic. 10 m thick.||||Overlies Tanami Complex, Gardiner Sandstone, Antrim Plateau Volcanics. Equivalent to Hazlett beds.|Quartz sandstone; minor siltstone, conglomerate.|
72579|Larranganni beds|69432|6|Mentioned|p17:2|Mesozoic|Mesozoic|||||Overlies Birrindudu Group.||12-JUL-16
74726|Larranganni beds""|64580|6|Mentioned|map legend|||Mesozoic sedimentary rocks, eastern Canning Basin.||||||27-JAN-09
41436|Larry Creek Formation|50436|6|Mentioned|p2.1|||Conformably underlies Fingoon Quartzite.||||||17-APR-08
80940|Late Merougil Group|72049|4|Described|p251, p254, p256, p259|||Kalgooglie Terrane. See also p260, p264, p266-p267, p270, p272.|c. 2665-2658 Ma||||Coarse felsic conglomerate with abundant volcanic quartz; massive, very coarse-grained quartzofeldspathic sandstone.|
69756|Latitude Hill gabbro/pyroxenite intrusion|44109|5|Briefly described|p9, p55-56|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Tectonic segment of Michael Hills gabbro. Gabbro and pyroxenite, olivine gabbro units with layers and lenses of olivine-bearing pyroxenite and rare peridotite.  Max. thick: ~8000m. ||||||
69756|Latitude Hill gabbro/pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. A segment of the Michael Hills gabbro intrusion.  Thickness: ~8000m.||||||21-SEP-05
27461|Laurel Beds|34287|6|Mentioned|p108|||L.Carb.||||||
27461|Laurel Beds|38263|6|Mentioned|p11|||||||||
27461|Laurel Beds|39796|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27461|Laurel Beds|44403|2|Defined|p.5,9,11,12||Dinantian|E/51-12. Dinantian. Calcarenite, sandstone, siltstone shelly calcarenite. fossils. U/lain probably unconformably Fairfield Beds, unconformably O/lain by Grant Formation.||||||
27461|Laurel Beds|44404|14|Not recorded|map legend||Carboniferous|||||||
27461|Laurel Beds|45056|6|Mentioned|p58|||L.Carb. Now U.Fairfield Fm.||||||
27461|Laurel Beds|45133|6|Mentioned|Fig.8|||||||||
27461|Laurel Beds|45143|6|Mentioned|Fig.3|||Time-stratigraphic interpretations.||||||
38131|Laurel Formation shale|23523|5|Briefly described|p1000|Carboniferous|Carboniferous|Formal name not intened.||||||
28671|Laurel Formation""|32638|6|Mentioned|p22|||Refers Playford & Lowry (1966)||||||
28671|Laurel Formation""|45143|6|Mentioned|p4|||||||||
80080|Laurel Sandstone|69312|6|Mentioned|p29 fig 37|||Canning Basin. Shown only as Laurel Ss, in about the middle of the Laurel Formation. probably meant to indicate a sandstone layer within the Formation. See also discussion on potential self-contained petroleum systems.||Laurel Formation||Overlies the Laurel Shale.||22-SEP-17
40309|Laurel Shale|24390|5|Briefly described|p8|||Geological Province: Canning Basin.||||||
40309|Laurel Shale|50085|6|Mentioned|p8|||Intended as Laurel Formation?  Geological Province: Canning Basin.||||||
40309|Laurel Shale|69312|6|Mentioned|p29 fig 37|||Canning Basin. Shown only as Laurel Sh, at the base of the Laurel Formation. Probably meant to indicate a shale layer within the Formation. See also discussion on potential self-contained petroleum systems.||Laurel Formation||Overlain by the Laurel Sandstone.||22-SEP-17
31930|Laurel beds|43876|14|Not recorded|p567|||Visean?||||||
39283|Laurel limestone|24246|6|Mentioned|p14|||Informal name. Geological Province: Canning Basin.||||||
39293|Laurel sandstone|24246|6|Mentioned|p14|||Geological Province: Canning Basin.||||||
83150|Laverton Group|72491|6|Mentioned|p5 Fig.4|||Kurnalpi Terrane, Yilgarn Craton.||||||
27182|Lawford beds|7433|5|Briefly described|p48 Fig.43, p50. |Tertiary|Tertiary|Fitzroy River catchment area, Canning Basin. Fluviatile unit.|||||Calcretes; algal stromatolites.|
27182|Lawford beds|38878|6|Mentioned|Map legend|Pliocene|Miocene|Miocene - Pleistocene||||||
27182|Lawford beds|41864|4|Described|p154|||||||||
27182|Lawford beds|41866|5|Briefly described|Map legend|Miocene||||||||
27182|Lawford beds|42771|5|Briefly described|p15, Fig.16|||||||||
27182|Lawford beds|43299|6|Mentioned|Map Legend||Tertiary|||||||
27182|Lawford beds|43300|5|Briefly described|Map Legend||Tertiary|||||||
27182|Lawford beds|43301|6|Mentioned|Map Legend||Tertiary|||||||
27182|Lawford beds|43302|6|Mentioned|Map Legend||Tertiary|||||||
27182|Lawford beds|45153|2|Defined|App.11-163|Quaternary|Quaternary|See also Table 1, P4.||||||
27182|Lawford beds|45158|3|Fully described|p10|||See also P34||||||
27182|Lawford beds|61155|5|Briefly described|p4, p16|Late Miocene|Middle Miocene|Age: 12.5-10Ma. Thickness: 24m (in Fitzroy Graben). Geological Province: Canning Basin and the Fitzroy Graben region. ||||||
80941|Lawlers Basalt|70275|6|Mentioned|p471|||The lowermost stratigraphic unit in the Agnew area, Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||||
80941|Lawlers Basalt|70276|6|Mentioned|p784|||The local name in the Agnew area (Agnew-Wiluna greenstone belt, Yilgarn Craton) for McFarlanes Basalt.||||||
80941|Lawlers Basalt|72049|6|Mentioned|p259|||Kalgoorlie Terrane.||Kambalda Sequence||||
38584|Lawlers Conglomerate|23782|5|Briefly described|p29 Fig. 21|||Geological Province: Yilgarn Craton.||||||
38584|Lawlers Conglomerate|70773|6|Mentioned|p60|||||||||
40773|Lawlers Tonalite""|24494|5|Briefly described|p13|Archean|Archean|Age: 2652 +/- 20 Ma (Rb-Sr whole rock age; Cooper et al., 1978). Informal - see Lawlers Tonalite||||||07-NOV-08
38585|Lawlers Ultramafic|23782|5|Briefly described|p29 Fig. 21|||Geological Province: Yilgarn Craton.||||||
41115|Lawlers greenstone formation|24196|6|Mentioned|p68|||Informal name - see also Lawlers Greenstone. Geological Provnce: West Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||
25157|Lawlers leucotonalite|35681|6|Mentioned|p42|||||||||
25157|Lawlers leucotonalite|38512|6|Mentioned|Table III|||||||||
28674|Le Lievre Beds|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|Adelaidean or Carpentarian||||||
28674|Le Lievre Beds|30533|4|Described|p19|||On Table 4||||||
28674|Le Lievre Beds|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28674|Le Lievre Beds|44155|5|Briefly described|p249 Tb.3-9|||900m thick. Appears as Le Lievre beds.|||||Quartzite, phyllite, sandstone.|
77224|Leake Spring Metamorphic Suite|66299|6|Mentioned|p215.|||Attributed to Williams et al., 1983; Williams, 1986. The rocks now grouped in Pooranoo Metamorphics and Leake Spring Metamorphics were included in this unit, but subsequently separated on the basis of different depositional ages.||||||15-OCT-12
25159|Learmonth Formation "upper"|42615|6|Mentioned|p20|||Variation on Learmonth Formation.||||||
41890|Leederville Formation, lower|12758|6|Mentioned|p30|||Informal - see Leederville Formation.||||||
70225|Leederville Formation, upper|24410|5|Briefly described|p28|Cretaceous|Cretaceous|Informal name. Of the Warnbro Group||||||
80807|Leederville Sequence|71958|6|Mentioned|p48|||Vlaming Sub-basin.||||||
69195|Leeuwin gneiss|24542|5|Briefly described|p7|Neoproterozoic|Mesoproterozoic|Not intended as a formal name. Pink feldspar-hornblende gneiss. Of Leeuwin Complex.||||||
70737|Lefroy Beds''|62453|6|Mentioned|p17|||Informal name||||||
70738|Lefroy beds''|62453|6|Mentioned|p17|||Informal name.||||||
75919|Leilera Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Sulphur Springs Group. Age shown as c.3255 Ma. Siliciclastic sedimentary rocks, minor felsic volcanic rocks, and chert; metamorphosed.||||||
83926|Leinster granodiorite|70276|6|Mentioned|p787|||Perseverance area, Agnew-Wiluna greenstone belt, Yilgarn Craton. Emplacement was coeval with D2 regional deformation.||||||
37890|Leinster monzogranite|24135|6|Mentioned|p7 Fig. 3|||Informal name.||||||
25163|Lennard Grinodiorite|41987|6|Mentioned|p73|||||||||
38836|Lennard River Group""|24061|4|Described|p180|Late Devonian|Middle Devonian|Informal name. Geological Province:  Canning Basin.||||||
68829|Lennis Formation|23571|5|Briefly described|p30|Carboniferous|Carboniferous|Probably misspelt - should be Lennis Sandstone? Geological Province: Officer Basin.||||||16-MAY-05
68829|Lennis Formation|61272|5|Briefly described|p122 Fig.3|||Overlies the Table Hill Volcanics. See also Lennis Sandstone.||||||
68829|Lennis Formation|62453|5|Briefly described|p5 Fig. 3|Ordovician|Ordovician|Geological Province: Gunbarrel Basin||||||13-OCT-08
68829|Lennis Formation|64103|6|Mentioned|p400 Fig. 3|Ordovician|Ordovician|Geological Province: Officer Basin.||||||07-FEB-11
68829|Lennis Formation|69003|6|Mentioned|p60|Ordovician|Ordovician|Officer Basin.||||||
68829|Lennis Formation|69445|6|Mentioned|p30:5, 17|||Officer Basin.||||Overlies Table Hill Volcanics.||12-JUL-16
68829|Lennis Formation|70772|6|Mentioned|p11|Ordovician|Ordovician|Officer Basin. Age is a detrital zircon maximum depositional age.|c. 520 Ma (Haines et al, 2013)|||||
38167|Lennnard Granite|23722|6|Mentioned|p11|||Misspelt - see Lennard Granite||||||
39662|Leo member, upper|24449|6|Mentioned|p745|||Informal - see Leo Member.||||||
82961|Leonora Sequence|73238|6|Mentioned|p4|||Kalgoorlie Terrane.||||||28-MAR-22
78679|Lesuer Sandstone|24160|6|Mentioned|p94|Triassic|Triassic|[Misspelling of Lesueur].||||||
80032|Lesueur Member, Lower|67888|6|Mentioned|p16|||||||||
25164|Lewin Shale|22701|6|Mentioned|p39|Neoarchean|Neoarchean|Superseded by Jeerinah Formation and Marra Mamba Iron Formation (Williams, 1989).||||||07-NOV-08
25164|Lewin Shale|23570|4|Described|p129|Archean|Archean|See also p235 App. 1.  Obsolete name originally used for the combined units of Jeerinah Formation and Marra Mamba Iron Formation.  Overlain by Carawine Dolomite : underlain by Little de Grey Lava. Max.thickness: 244m.||||||07-NOV-08
25164|Lewin Shale|23585|5|Briefly described|p14 Fig 5|Archean|Archean|Replaced by Jerrinah Formation. Of Fortescue Group. Underlying unit Baramine Volcanic Member. Geological Province: Hamersley Basin.||||||07-NOV-08
25164|Lewin Shale|23594|5|Briefly described|p9 Fig 6|Mesoproterozoic|Paleoproterozoic|Replaced with Jeerinah Formation. Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
25164|Lewin Shale|23745|5|Briefly described|p7 Fig 5|Proterozoic|Proterozoic|Replaced by Jeerinah Formation.||||||
25164|Lewin Shale|23746|5|Briefly described|p8 Fig 5|Proterozoic|Proterozoic|Renamed Jeerinah Formation. Of Fortescue Group.||||||
25164|Lewin Shale|29845|6|Mentioned|Plate 3|||||||||
25164|Lewin Shale|29850|6|Mentioned|p1020|||||||||
25164|Lewin Shale|30503|5|Briefly described|Table 1|||||||||
25164|Lewin Shale|33544|6|Mentioned|p31|||See also PP84, 280 & 281. Correlation||||||
25164|Lewin Shale|34135|5|Briefly described|Table 2|||Lower Proterozoic.||||||
25164|Lewin Shale|35269|6|Mentioned|p304|||||||||
25164|Lewin Shale|36551|6|Mentioned|Table 23|||||||||
25164|Lewin Shale|36882|6|Mentioned|p129|||||||||
25164|Lewin Shale|37460|3|Fully described|Table 3.I|||||||||
25164|Lewin Shale|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25164|Lewin Shale|39426|4|Described|p11|||||||||
25164|Lewin Shale|39697|6|Mentioned|p123|||||||||
25164|Lewin Shale|40369|6|Mentioned|Table 1|||||||||
25164|Lewin Shale|41669|6|Mentioned|p25|||||||||
25164|Lewin Shale|42352|6|Mentioned|p5|||As used by Hickman 1978. Now divided into Jeerinah Formation and Marra Mamba Iron Formation.||||||
25164|Lewin Shale|42785|6|Mentioned|p262|||||||||
25164|Lewin Shale|43595|6|Mentioned|Table 2-29,p219|||'superseded name'?||||||
25164|Lewin Shale|44152|6|Mentioned|p173, p176 Fig.2-154||||||Baramine Volcanic Member|Is overlain by Carawine Dolomite.||
25164|Lewin Shale|44297|14|Not recorded|p.5,7,8-9|||(F51-9). See also p. 10,12,18,19,20,21,map.||||||
25164|Lewin Shale|44298|14|Not recorded|map legend||Proterozoic|||||||
25164|Lewin Shale|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group. Partly correlated with Jeerinah Formation.||||||07-NOV-08
25164|Lewin Shale|44503|14|Not recorded|p.7|||Correlates with Marra Mamba Iron Formation & Jeerinah Formation. (F50-12).||||||
25164|Lewin Shale|46319|4|Described|p14|Proterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
25164|Lewin Shale|50544|6|Mentioned|p44 Fig. 8|Archean|Archean|Of Hickman et al (1983).  Superseded by Jeerinah Formation.||||||07-NOV-08
25164|Lewin Shale|60429|5|Briefly described|p20 Fig. 5, p21|Archean|Archean|Of Hickman et al (1983). Superseded by Jeerinah Formation.||||||07-FEB-11
25164|Lewin Shale|60635|6|Mentioned|p51 Fig. 2.2A|||Now referred to as the Jeerinah Formation of Thorne and Hickman, 1998||||||29-JUN-05
25164|Lewin Shale|65683|5|Briefly described|p799|||Correlated with Marra Mamba Iron Formation? Shallow water sediments.||||||
25164|Lewin Shale|67183|6|Mentioned|p643|||Of de la Hunty (1965), Hickman (1978). Now called Jeerinah Formation.||||||
25164|Lewin Shale|67229|6|Mentioned|p3 Fig.2|||de la Hunty (1964) gave this name to rocks mapped (by Noldart and Wyatt, 1962) as part of Carawine Dolomite and Tumbiana Pisolite. Renamed as Jeerinah Formation by MacLeod and de la Hunty (1965).||||||
29960|Lewin Shale""|43055|6|Mentioned|Table 1|||refers to de la Hunty (1964).||||||
42103|Lewis granite|23809|6|Mentioned|p5 Tb. 2|Proterozoic|Proterozoic|Of the Frederick Suite.  Informal name.||||||
77528|Liberty Bore Complex|66880|6|Mentioned|p17. |Archean|Archean|An informal name for a unit in Kurnalpi Sequence, Kurnalpi Terrane.|2712 +/- 5 Ma.||||Includes rhyolite.|
38652|Liberty Bore complex|23786|5|Briefly described|p20|Archean|Archean|Informal name.  Age: 2708+/-6Ma (SHRIMP).  Geological Province: Yilgarn Craton.||||||07-NOV-08
38652|Liberty Bore complex|24196|5|Briefly described|p48|Archean|Archean|Age: 2708 +/- 6 Ma (Nelson, 1995).||||||07-NOV-08
23725|Liberty Granite|41371|5|Briefly described|p21|||Mention Fig.1||||||
32740|Lightjack-Noonkanbah Formation|44998|14|Not recorded|p.110|||||||||
38702|Lillybooroona Conglomerate|23722|4|Described|p34|Early Carboniferous|Late Devonian|Max. thickness: 60m.   Geological Province: Canning Basin||||||
80496|Limbunyah Group|63866|5|Briefly described|p92|||Birrindudu Basin. Age derived from intercalated volcanics.|c. 1635 Ma|||Overlies the Gardiner Sandstone.||
80496|Limbunyah Group|72718|6|Mentioned|p7-8|||Birrindudu Basin. Equivalent to McArthur Group.|||Killaloc, Fraynes, Blue Hole, Amos Knob, and Margery formations. Campbell Springs, Mallabah, and Pear Tree dolostones. Farquharson and Stirling sandstones. Kunja Siltstone.|Unconformably[?] overlain by Wickham Formation (Wattie Group).||
80496|Limbunyah Group|73184|6|Mentioned|p194|Statherian|Statherian|Tanami region.|ca 1.64 Ga||||Includes volcanics.|
81378|Lindsay Basalt|70326|4|Described|p360,363-364|Neoarchean|Neoarchean|Geological province: Coolgardie Domain, Kalgoorlie Terrane, Yilgarn Craton. Correlable to Missour, Never Can Tell and Centenary Bore basalts.||||Overlain by Hampton Formation. Underlain by Brilliant Ultramafic. Intruded by Three Mile Sill.|Pillowed high-Fe tholeiite intercalated with several thin sediment intervals.|15-AUG-19
23728|Linger and Die Group|22534|5|Briefly described|p8, Fig.4 p7|||Previously called the 'Siberia Complex'||||||
23728|Linger and Die Group|22596|6|Mentioned|Fig.9 p419|||||||||
23728|Linger and Die Group|23132|6|Mentioned|p336|||||||||
23728|Linger and Die Group|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
23728|Linger and Die Group|42221|5|Briefly described|Table 1 P6|||||||||
23728|Linger and Die Group|42382|6|Mentioned|Table 1 P9|||||||||
23728|Linger and Die Group|42696|6|Mentioned|Plate 1B|||||||||
23728|Linger and Die Group|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23728|Linger and Die Group|42989|5|Briefly described|Table 1, Fig.2|||||||||
23728|Linger and Die Group|43074|6|Mentioned|Table 1|||||||||
23728|Linger and Die Group|43101|5|Briefly described|Table 1.|||||||||
23728|Linger and Die Group|43162|6|Mentioned|5|||||||||
23728|Linger and Die Group|43496|6|Mentioned|6|||||||||
23728|Linger and Die Group|60514|5|Briefly described|p65 Table 1.|Archean|Archean|Includes: Big Dick Basalt, Siberia Komatiite, Walter Williams Fm. Overlain by Grants Patch Group, underlain by Pole Group. Geol Prov: Ora Banda Domain. High-Mg basalt at top then thin komatiite flows, overlying thicker komatiite flows.||||||07-FEB-11
23728|Linger and Die Group|60627|5|Briefly described|p65 Tb.1|||||||||
23728|Linger and Die Group|65204|5|Briefly described|pg6 Tbl.1|Archean|Archean|Includes Big Dick Basalt, Siberia Komatiite and Walter Williams Formation. Thin komatiitic basalt at top, thin komatiitic flows with minor interflow sedimentary beds overlying thicker komatiitic flows and/or massive olivine adcumulate.||||||11-JUN-15
23728|Linger and Die Group|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.|||Big Dick Basalt, Siberia Komatiite, Walter Williams Formation.||Massive olivine adcumulate and/or thick komatiite flows, overlain by thin komatiite flows with minor interflow sedimentary beds; high Mg basalt at top.|
23728|Linger and Die Group|73391|6|Mentioned|Appendices.|||Witt (1990). Regional stratigraphic correlation chart of other workers.|||Big Dick Basalt, Siberia Komatiite.|||
28683|Little De Grey Lava""|39697|6|Mentioned|p15|||||||||
78506|Little Gap Mafic-Ultramafic Suite|68110|6|Mentioned|p674 Fig. 2|||Variation on Little Gap Suite (p687).||||||
30671|Little Gold River Microgranodiorite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
30671|Little Gold River 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
30671|Little Gold River Microgranodiorite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
30671|Little Gold River Microgranodiorite|43281|5|Briefly described|Map legend|Proterozoic|Proterozoic|Approx 1865 - 1850 Ma.||||||
30671|Little Gold River Microgranodiorite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite. Microgranodiorite (micro quartz diorite), and orthopyroxene-bearing andesite porphyry. Age: c.1865-1850Ma. In the Hooper Complex and Lamboo Complex western zone.||||||07-NOV-08
30671|Little Gold River Microgranodiorite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
30671|Little Gold River Microgranodiorite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Microgranodiorite (micro quartz diorite), and orthopyroxene-bearing andesite porphyry.|
30671|Little Gold River Microgranodiorite|72437|5|Briefly described|p37|||Whole-rock analyses are provided.|||||Micro-diorite.|
27466|Little Gold River Porphyry|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27466|Little Gold River Porphyry|32728|5|Briefly described|p23|||See also Fig.3||||||
27466|Little Gold River Porphyry|36885|4|Described|p171|||||||||
27466|Little Gold River Porphyry|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
27466|Little Gold River Porphyry|44155|5|Briefly described|p234 Tb.3-2, p239, p241 Tb.3-4|Paleoproterozoic|Paleoproterozoic|||||Intrudes Whitewater Volcanics. Overlain by O'Donnell Formation unconformably.|Dark-grey orthopyroxene-feldspar porphyry with sporadic quartz; abundant angular xenoliths.|
27466|Little Gold River Porphyry|44366|14|Not recorded|p.11, Table 1||Carpentarian|||||||
27466|Little Gold River Porphyry|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971).||||||
27466|Little Gold River Porphyry|44397|14|Not recorded|p.9,18,19, Table 2||Carpentarian|||||||
27466|Little Gold River Porphyry|44398|14|Not recorded|map legend||Carpentarian|||||||
27466|Little Gold River Porphyry|48931|6|Mentioned|p33|||Correlation||||||
38092|Little de Grey Lava""|23570|6|Mentioned|p239 Appendix 1|||See Little de Grey Lava.||||||
38087|Little de Grey Lava, "Upper"|23570|6|Mentioned|p236 Appendix 1|||See also Little de Grey Lava.||||||
32887|Liveringa Beds|48848|14|Not recorded|p.44|||||||||
32766|Liveringa member|45016|14|Not recorded|Not recorded|||Tb. at back. Correlates with Coolkilya Greywacke.||||||
28686|Liverynga Group|33711|6|Mentioned|Table 4|||Mis-spelling of Liveringa.||||||
38697|Lizard Hills Formation""|23789|5|Briefly described|p62|||Geological Province: Pilbara Craton.||||||
80495|Loadstone monzogranite|63866|5|Briefly described|p132|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1827 Ma|Sally Downs Supersuite||||
40199|Locker Formation|24203|5|Briefly described|p301|Early Triassic|Early Triassic|Thick shales.  Same as Locker Shale?   Geological Province Carnarvon Basin.||||||
40199|Locker Formation|65708|5|Briefly described|p107|Triassic|Triassic|North West Shelf. An important secondary source; mainly gas-prone. Scythian-Ladinian age.|||||Deltaic shales.|29-JUN-22
67871|Londonderry pegmatite|60076|6|Mentioned|p37|||Informal name.  On YILMIA sheet.  Has yielded beryl, lepidolite, petelite and tantalite-columbite.||||||02-FEB-05
67871|Londonderry pegmatite|65834|6|Mentioned|p49, 61|||Located 19km SSW of Coolgardie, Kalgoorlie Terrane. Lensoid to sheet-like body; up to 25m thick. Has produced microcline feldspar, lepidolite, beryl, amblygonite and petalite (quantities given). Appears formalised as Londonderry Pegmatite on p49.|||||Li-rich granite pegmatite.|
22212|Lone Hand Granite|22534|6|Mentioned|p12|||||||||
22212|Lone Hand Granite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
22212|Lone Hand Granite|43214|6|Mentioned|Map Legend||Archean|||||||07-NOV-08
83650|Long Point dyke|73480|5|Briefly described|p208, p216-218|Cambrian|Neoproterozoic|Intruded sheared ortho- and paragneisses. Youngest inherited U-Pb age of 910+/-10 Ma is very slightly discordant. Likely associated with Kuunga Orogeny. See also Long Point basaltic dyke.|ca 910+/-10 Ma U-Pb zircon maximum age||||Porphyritic basalt predominantly comprised of strongly sericitised plagioclase phenocrysts in a highly altered groundmass. Unmetamorphosed.|
28692|Loongana Conglomerate""|30012|6|Mentioned|p18|||Refs Fairbridge (1953)||||||
28692|Loongana Conglomerate""|30563|6|Mentioned|p11|||Refers Fairbridge (1953).||||||
28692|Loongana Conglomerate""|30564|6|Mentioned|p11|||Refers Fairbridge (1953), Lowry (in press).||||||
28692|Loongana Conglomerate""|31902|6|Mentioned|p4|||Refers Fairbridge (1953)||||||
28692|Loongana Conglomerate""|31904|6|Mentioned|p4|||Refers Fairbridge (1953)||||||
28692|Loongana Conglomerate""|31906|6|Mentioned|p7|||Refers Fairbridge (1953)||||||
28692|Loongana Conglomerate""|31907|6|Mentioned|p4|||Refers previous authors. Now Loongana Sst.||||||
28692|Loongana Conglomerate""|31908|6|Mentioned|p7|||Refers Fairbridge (1953)||||||
28692|Loongana Conglomerate""|31909|6|Mentioned|p4|||Now Loongana Sst.||||||
28692|Loongana Conglomerate""|32552|6|Mentioned|p46|||Refers Fairbridge (1953)||||||
28692|Loongana Conglomerate""|33586|6|Mentioned|p13|||Refers Fairbridge (1953).||||||
28692|Loongana Conglomerate""|33589|6|Mentioned|p7|||Previously Loongana Sst.||||||
28692|Loongana Conglomerate""|33595|6|Mentioned|p15|||Refers Fairbridge 1953 & McWhae et al. 1958||||||
28692|Loongana Conglomerate""|35496|6|Mentioned|p20|||Now known as Loongana Sandstone||||||
28692|Loongana Conglomerate""|36890|6|Mentioned|p412|||Renamed Loongana Sandstone||||||
28692|Loongana Conglomerate""|44133|6|Mentioned|p134|||Superseded by Loongana Formation. ||||||
26702|Loongana sandstone|34192|6|Mentioned|Map legend|Cenomanian|Albian|Cenomanian - Aptian||||||
78429|Loongara Sandstone|65194|6|Mentioned|p31|||High groundwater salinity.||||||
23739|Lordy Basalt|42533|3|Fully described|p55, p58|||Name reserved.||||||
23739|Lordy Basalt|44149|5|Briefly described|p35 fig 2-30, p38-39|Archean|Archean|Of Murchison Province||Porlell Subgroup||Overlain by Stockyard Basalt.|A sequence of high-Mg basalt (with needle-spinifex texture) and associated mafic and ultramafic sills.|
23739|Lordy Basalt|64891|5|Briefly described|p37 Fig. 2|Archean|Archean|Superseded by Lordy Basalt Member. Geological province: Murchison Domain.||||||07-FEB-11
23739|Lordy Basalt|65268|6|Mentioned|p6 fig 4|||||Porlell Subgroup|||Mainly high-Mg basalt.|
23739|Lordy Basalt|70030|6|Mentioned|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Coodardy Formation.||||
69027|Lotus diorite|60978|6|Mentioned|p68-69 Fig.3|||Informal reference to a dolerite in the Bronzewing gold deposit area. Geological Province: Yilgarn Craton.||||||
70134|Louden Volcanic Member|63441|5|Briefly described|p5 Tb.1|Archean|Archean|Of Bookingarra Formation (Croydon Group, Pilbara Supergroup). Geological province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
70134|Louden Volcanic Member|63538|4|Described|p32, p33, p34, p35|Archean|Archean|Of Bookingarra Formation. Geological Province: Pilbara Craton. Locally includes aphyric flow units and cumulate-textured units but is dominated by well-developed pyroxene-spinifex textures.||||||17-APR-13
70134|Louden Volcanic Member|64174|5|Briefly described|Map legend|Archean|Archean|Of the Bookingarra Formation (Croydon Group, De Grey Supergroup).  Geological province: Mallina Basin. Basalt and komatiite, with locally thick siliciclastic sedimentary intercalations; metamorphosed.||||||07-NOV-08
70134|Louden Volcanic Member|64580|4|Described|map legend||Mesoarchean|Of Bookingarra Formation. Basalt and komatiite, with locally thick siliciclastic sedimentary intercalations; metamorphosed.||||||15-DEC-08
70134|Louden Volcanic Member|64632|6|Mentioned|p203|Mesoarchean|Mesoarchean|Compared with basalts on northern (Salt Well Member) & NE (Coonieena Basalt Member) margins of East Pilbara Terrane||Of the Bookingarra Formation|||Spinifex and variolitic textured basalts.|08-SEP-15
70134|Louden Volcanic Member|67201|4|Described|p16-17 Fig.9, p21 Fig.12, see comments|Archean|Archean|In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin. "Louden Volcanics" mentioned on p24 in previous interpretations section. Shortened to Louden Volcanics in some figures. Page location continued: p23-24, p57-59, p63, p65.||Bookingarra Formation||Louden Volcanic and Mount Negri Volcanic Members overlie (and overlap with) Rushall Slate in Whim Creek greenstone belt.|Intrusions. Siliceous high-Mg basalt; basalt and komatiite (non-variolitic and coarse pyroxine spinifex textures), with locally thick siliciclastic sedimentary intercalations; metamorphosed.|
70134|Louden Volcanic Member|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Bookingarra Formation.|||Basalt and komatiite, with locally thick siliciclastic sedimentary intercalations; metamorphosed|
70134|Louden Volcanic Member|69301|5|Briefly described|p15|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Mallina Basin.||Bookingarra Formation|||Siliceous high-Mg basalt.|
70134|Louden Volcanic Member|69590|4|Described|GEOL_LUT_CSV files|||Geological province: Pilbara Craton. Of De Grey Superbasin. Events: North Pilbara Orogeny. See 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2964-2943 Ma (isotopic)|Unit of Bookingarra Formation.|||Basalt and komatiite, with locally thick siliciclastic sedimentary intercalations; metamorphosed|
70134|Louden Volcanic Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt, komatiitic (high-mg) basalt, sandstone, conglomerate|
70134|Louden Volcanic Member|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.||Bookingarra Formation|||Basalt and komatiite, with locally thick siliciclastic sedimentary intercalations; metamorphosed.|
70134|Louden Volcanic Member|72668|6|Mentioned|p14-15|||Basalts similar to this occur across the Mallina Basin.||Bookingarra Formation.||Overlies the Cistern Formation.|Locally spinifex-textured and variolitic basalts.|
73780|Louge Brook Granite|50542|6|Mentioned|p131|Archean|Archean|A pluton of the Wheatbelt Batholith. Age: 2612+/-5Ma. Geological Province: Yilgarn Craton.||||||07-FEB-11
41579|Louisa Downs group|22496|6|Mentioned|p10|||Informal name.||||||
42199|Lower Basalt|50421|4|Described|p285, 286 Fig.2||Archean|Overlain by unassigned komatiite. High Mg to tholeiitic. Kalgoorlie Terrane. Eastern Goldfields Superterrane (probably equivalent to Eastern Goldfields Province). Overlain by unassigned komatiite. >2702+-4 Ma.||||||07-NOV-08
42199|Lower Basalt|73391|5|Briefly described|p17, 19, 39, 48, 51, 167, 174, 177, 194|||See also p242, 244, 247, 266, 268, 272, 278-279, 284-286, 304, 306, 330, 347-348, Appendices. Swager et al. (1990); their lowest unit in the Kalgoorlie Terrane (Eastern Goldfields Province). Also appears as Lower basalt on p19 and 51, and as Lower Basalt Group on p39. Occasionally referred to as the Lower Basalt Unit. Equivalent to the Scotia Basalt (in the Boorara Domain).|||Missouri, Wongi, Lunnon Basalts.|Overlies Burbanks Basalt. Is overlain in the various Domains by Siberia Komatiite, Hampton Ultramafic, Kambalda Komatiite, Mount Pleasant Sill and Big Blow Chert.|Basaltic volcanic rocks and co-magmatic mafic intrusive sills that include high-Mg (komatiitic basalt) and tholeiitic compositions.|
31384|Lower Birdrong Sandstone|43564|6|Mentioned|p462|||Informal variation on Birdrong Sandstone||||||
33929|Lower Capricorn Megasequence|22512|6|Mentioned|Fig1 P284|||||||||
31426|Lower Carbonate Member|43599|6|Mentioned|p247|Early Silurian|Early Silurian|Worral Formation||||||
83076|Lower Chert Member|73160|6|Mentioned|p3, p5 Fig.3|||Commonly known as the North Pole Chert.||Dresser Formation||||
77125|Lower Dupuy Sands|61554|6|Mentioned|p625 Fig.2|||Barrow Island.||||||
31381|Lower Grant Sequence""|43563|6|Mentioned|p19|||Informal||||||
28696|Lower Greenstone group|30295|3|Fully described|p79|||||||||
32767|Lower Holmwood Shale""|45016|14|Not recorded|p.55|||May be equivalent of Weedarra Shale.||||||
32886|Lower Liveringa Formation|48848|14|Not recorded|p.85|||||||||
32742|Lower Liveringa beds|44998|14|Not recorded|App.4 p282-3|||Contains Lightjack & Balgo Members.||||||
77186|Lower Malu Formation|44139|6|Mentioned|p281 Table 3-15|||Informal name (of Turner 1983 PhD thesis). Same as Malu Quartzite of Chin et al (1982).| | ||||10-SEP-12
34112|Lower Mannum Formation|22626|6|Mentioned|446 fig 10 447|Early Miocene|Late Oligocene|Geol province Murray Basin. Overlying unit Upper Mannum Formation, underlying unit Ettrick Formation||||||
34110|Lower Morgan Limestone|22626|6|Mentioned|446 fig 10|Middle Miocene|Middle Miocene|Geol province Murray Basin. Overlying unit Upper Cadell Marl, underlying unit Finnis Clay||||||
77188|Lower Vale Shale|44139|6|Mentioned|p281 Table 3-15|||Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation.| | ||||10-SEP-12
32789|Lower unit|44230|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
32789|Lower unit|44231|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
79547|Lower"" Coongan Volcanics|67229|6|Mentioned|p3 Fig.2|||Noldart and Wyatt (1962). Obsolete name: rocks included in the Hardey Sandstone.||||||
28699|Lower"" Little De Grey Lava|36882|6|Mentioned|p124|||||||||
28699|Lower"" Little De Grey Lava|67229|6|Mentioned|p3 Fig.2|||Obsolete. Rocks included in Kylena Basalt Member (MacLeod and de al Hunty, 1965), renamed Boongal Pillow lava Member (de la Hunty, 1965), then Kylena Basalt (Kriewaldt and Ryan, 1967), then Kylena Volcanics (Williams, 1968) and Kylena Basalt again (Hickman, 1983).||||||
83946|Lowes Porphyry|70482|6|Mentioned|p324 Fig.5|Archean|Archean|Kanowna Belle mine, Eastern Goldfields Superterrane, Eastern Yilgarn Craton. Fig.5 shows the unit's exposure in the mine pit.|||||Felsic intrusion.|
77563|Lucky Supersequence|66937|5|Briefly described|p155, pp172-173.|Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin. Poor outcrops in a syncline 42 km long by 2 km wide.|||||Conglomerate with sandstone lenses; graded massive to plane-bedded coarse- and medium-grained pebbly sandstone; massive to laminated mudrock; silicified shale.|
77563|Lucky Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
23744|Luke Creek Group|22517|6|Mentioned|P294||Archean|||||||07-NOV-08
23744|Luke Creek Group|22774|4|Described|p571, Fig.2 p573|||Age of unit 3.0Ga. See also Fig.1 p572, p573||||||
23744|Luke Creek Group|23135|5|Briefly described|p279 Fig.1||Archean|||||||07-NOV-08
23744|Luke Creek Group|23146|5|Briefly described|p149|||||||||
23744|Luke Creek Group|23148|5|Briefly described|p112 Table.2|||||||||
23744|Luke Creek Group|23441|5|Briefly described|p154|Archean|Archean|Of Murchison Supergroup.||||||15-JUN-09
23744|Luke Creek Group|23569|5|Briefly described|p7 Tb. 2|||||||||
23744|Luke Creek Group|23592|6|Mentioned|p7|||||||||
23744|Luke Creek Group|23597|6|Mentioned|p20 Table 4|||||||||
23744|Luke Creek Group|23744|6|Mentioned|p8|||||||||
23744|Luke Creek Group|23787|6|Mentioned|p22|||Geological Province: Murchison Terrane.||||||
23744|Luke Creek Group|23922|4|Described|p1234|Archean|Archean|Geological Province: Murchison-Southern Cross Terrane, Yilgarn Craton.  Overlain by Mount Farmer Group.  Min. age: 3010 +/- 7 Ma.||||||15-JUN-09
23744|Luke Creek Group|23955|6|Mentioned|p1240|||Geological Province: Murchison province, Yilgarn Craton.||||||
23744|Luke Creek Group|24160|5|Briefly described|p109, p114 Fig.50.|||Divided into lower and upper volcanic sequences.||Unit in Murchison Supergroup.|Includes Murrouli Basalt; Golconda, Gabanintha and Windaning Formations.|Is overlain unconformably by Mount Farmer Group.|Greenstone sequence.|
23744|Luke Creek Group|24295|5|Briefly described|p1228|Archean|Archean|Age: 2.8 Ga. Geological Province: Murchison province, Yilgarn Craton.||||||07-NOV-08
23744|Luke Creek Group|41885|6|Mentioned|p144|||||||||
23744|Luke Creek Group|42363|5|Briefly described|Fig. 1 P312, P313|||||||||
23744|Luke Creek Group|42533|3|Fully described|p10|||||||||
23744|Luke Creek Group|44149|5|Briefly described|p32, p33 fig 2-29, p34-38, p47, p49|Archean|Archean|See also p51-52, p56. Of Murchison Province. Intruded by monzogranite and granodiorite sheets; folded and formed pegmatite-banded gneiss. Compositions of volcanic rocks detailed. Several ages given. Deformation episodes detailed.|c.3.0 Ga (eruption).|Murchison Supergroup|Murrouli Basalt; Golconda, Gabanintha, Windaning Formations.|Is overlain by Mount Farmer Group unconformably.|Greenstone sequence.|
23744|Luke Creek Group|61144|5|Briefly described|p13|Archean|Archean|Of the Murchison Supergroup (lower succession).  Age: 3020-2930Ma (U-Pb zircon).  Geological Province: Murchison Province.||||||07-NOV-08
23744|Luke Creek Group|64771|6|Mentioned|p32|||Watkins and Hickman (1990). Lower part of the Polelle Syncline, Abbotts greenstone belt.||||||
23744|Luke Creek Group|64891|5|Briefly described|p36|||Formerly part of the original "Murchison Supergroup" - its Luke Creek and Mount Farmer Groups now replaced by Norie, Polelle and Glen Groups as presented by Van Kranendonk (2008). Age: 2950Ma. Discussion of greenstone belt age correlations (p36).||||||07-FEB-11
23744|Luke Creek Group|65268|5|Briefly described|p4-7, Figs.3,4|||Basal greenstones in Murchison Domain. Consisted of 4 Formations comprising 2 volcanic sequences; one tholeiitic/komatiitic the other ultramafic.||Murchison Supergroup|Includes Murrouli Basalt; Golconda, Gabanintha and Windaning Formations.|Overlain by Mount Farmer Group.|Tholeiitic and komatiitic basalt, BIF and interlayered mafic rocks; ultramafic interlayered tholeiitic and komatiitic basalt, mafic and felsic volcanic rocks and associated sedimentary rocks, and jaspilitic BIF.|
23744|Luke Creek Group|68110|5|Briefly described|p671|Mesoarchean|Mesoarchean||c. 3000-2800 Ma|Lower unit in the Murchison Supergroup.||||
23744|Luke Creek Group|69267|5|Briefly described|p651-654|||Murchison Province, Yilgarn Craton. Occurs within greenstone belts. Underwent multiple deformation events.||Murchison Supergroup.|Murrouli Basalt; Golconda, Gabanintha, Windanning Formations.|Is overlain unconformably by Mount Farmer Group.||
23744|Luke Creek Group|70269|5|Briefly described|p105-106, 122|Archean|Archean|Yilgarn Craton. Hosts almost all significant mineralisation in the Murchison Province, mainly from the Meekatharra Mt. Magnet greenstone belt. Mineralisation assemblages described and discussed. Sulfide Pb isotope studies (detailed) indicate two mineralisation events c.300 m.y. apart.|c.3000 Ma.||||Murchison Province, Yilgarn Craton. Includes foliated tholeiitic metabasalts and metadolerites, and ubiquitous felsic intrusive bodies. Garnet schists, cordierite-muscovite schists; quartz-biotite +/- sulfide alteration.|
23744|Luke Creek Group|70270|5|Briefly described|p518, Fig. 1|Mesoarchean|Mesoarchean|Of Myers (1990), Watkins  and Hickman (1990). Murchison Province.|~3.0 Ga||p518-519 appears to say that the Minjar Group, Thundelarra Group and Gossan Hill Group of Clifford, 1992 are part of the Luke Creek Group[??].|||26-JUN-18
23744|Luke Creek Group|70281|5|Briefly described|p454-455, 470|||Southern Cross terrane, Yilgarn Craton. Hosts the Nevoria gold skarn deposit. More often than not is referred to as Luke Creek succession or Luke Creek greenstones.|3023 +/- 10 Ma (minimum; Nelson, 1999).|||Is overlain unconformably by the Marda volcano-sedimentary complex.|Greenstones; basalt-komatiite-graywacke succession.|
23744|Luke Creek Group|70796|6|Mentioned|site_lithology.csv||||||||Banded ironformation and amphibolite derived from intrusive rock.|
31698|Luluigni Formation|43818|6|Mentioned|Fig.2.p39||Late Devonian|||||||
74865|Lululgui Formation|64643|5|Briefly described|p3 Fig. 2|Upper Devonian|Upper Devonian|Misspelling of Luluigui Formation.||||||
35657|Lumen Siltstone|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Speewah Group.||||||
70742|Lungkarta Formation, lower''|62453|6|Mentioned|p49|||Informal Name.||||||
40328|Lunnon Basalts|23924|6|Mentioned|p217 Fig. 9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
31395|Lunnon Formation|22682|5|Briefly described|Fig9,p14||Archean|||||||07-NOV-08
31395|Lunnon Formation|43629|5|Briefly described|p521|Archean||Misspelling/Variation. Yilgarn Craton. Age 2.7 Ga. (late Archaean)||||||07-NOV-08
41085|Lunnon basalt|24139|5|Briefly described|p239 Table 1|||Geological Province: Kambalda Domain.  Of the Kalgoorlie Group.||||||
41085|Lunnon basalt|62110|6|Mentioned|p1444|||Informal - see Lunnon Basalt.||||||07-FEB-11
76844|Lunnon metapicrite|66854|6|Mentioned|p944,  p947 Fig.5.|||||||||
70743|Lupton Beds''|62453|6|Mentioned|p45|||Informal name.||||||
73864|Lydia Mine Group|24391|6|Mentioned|p8-5 Fig.2|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
32757|Lyons Conglomerate|44344|14|Not recorded|p.3|||(G50-1).||||||
32757|Lyons Conglomerate|45015|6|Mentioned|p.7|||Of Maitland (1909). Superseded by Lyons Group.||||||29-JAN-08
38809|Lyons basalt|23931|6|Mentioned|p201 Table 1|||Informal name - see Lyons Basalt. Geological Province: Yilgarn Craton.||||||
38809|Lyons basalt|60979|5|Briefly described|p92, p86 Fig.2, p90|||Part of the Jundee sequence - Jundee goldfield area. Thickness: ~600-1200m. See also p91 Fig.4. Medium- to coarse-grained, ophtic to sub-ophitic and cumulate-textured dolerite, locally granophyric or pyroxenitic||||||27-JUN-05
38808|Lyons dolerite|23931|6|Mentioned|p201 Table 1|||Informal name - see Lyons Dolerite. Geological Province: Yilgarn Craton.||||||
38808|Lyons dolerite|60979|5|Briefly described|p86 Fig.2|||Informal name. Part of the Jundee sequence in the Jundee goldfield area. Geological Province: Yilgarn Craton. Medium- to coarse-grained, ophitic to sub-ophitic and cumulate-textured dolerite, locally granophyric or pyroxenite.||||||
70519|Lyons series|45015|5|Briefly described|p8|Early Permian|Early Permian|Of Raggatt and Fletcher (1937). Informal name - see Lyons Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
39907|Lyre Creek Agglomerate Member""|24353|5|Briefly described|p6|Archean|Archean|Refers to the Lyre Creek Member. Parent: Cliff Springs Formation. Geological Province: Pilbara Craton||||||07-NOV-08
39289|M. Australis Sandstone|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin||||||24-FEB-05
40314|M. australis Sand|50024|6|Mentioned|p13|||Informal name.  Hosts recoverable oil.  Geological Province: Carnarvon Basin.||||||
75241|M. australis Sandstone Member""|64973|6|Mentioned|p505|||Informal and obsolete. Of Delfos and Boardman (1994). Geological Province: Carnarvon Basin.||||||16-JUN-09
40781|M. australis sand""|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
40781|M. australis sand""|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Informal name.  Geological Province: Northern Carnarvon Basin (Dampier Sub-basin).||||||
72627|M. australis sands|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Within the Muderong Shale. Geological Province: Dampier Sub-basin.||||||08-NOV-06
25187|Mabel Downs Granite|31393|6|Mentioned|Pl.25|||||||||
25187|Mabel Downs Granite|43632|6|Mentioned|p6|||||||||
82051|Mabel Downs Granitoid|72437|6|Mentioned|p10|||Obsolete name, replaced by the Mabel Downs Tonalite.||||||
37106|Mabel Downs suite|23751|5|Briefly described|p16|Orosirian|Orosirian|Age: 1835-1815 Ma. Of Sally Downs supersuite.||||||
37106|Mabel Downs suite|66845|4|Described|p537 Fig.3, p538, p539, p541, p542 Fig.8|||||Sally Downs supersuite|Mabel Downs Tonalite, Sally Downs Tonalite, and McHale Granite||variably foliated, medium-grained, even-textured to porphyritic biotite-hornblende tonalite and quartz-diorite; some edenitic hornblende crystals have orthopyroxene cores; abundant mafic enclaves|
37106|Mabel Downs suite|66846|4|Described|p548-p559|Orosirian|Orosirian|Age range probably from U-Pb SHRIMP dating of zircon (see p547). See also:  most figures. Characterised by medium K2O. Rare earth element abundances given on p551 Tb. 2.|1835-1817 Ma|Sally Downs supersuite|||Hornblende and hornblende-biotite tonalite and quartz diorite; even-textured; foliated.|12-AUG-20
37106|Mabel Downs suite|72437|4|Described|p9, p11, p99-101|Palaeoproterozoic|Palaeoproterozoic|Occurs along the eastern margin of the central zone of the Lamboo Complex. Twenty analyses are presented for this suite. Ogasawara (1988) presented five analyses from this suite.|c. 1835-1815 Ma|Sally Downs supersuite|Includes the Sally Downs Tonalite, McHale Granodiorite and the Mabel Downs Tonalite.||Tonalites.|
82052|Mabel Hill Tonalite''|72437|6|Mentioned|p11|||One whole rock analysis is presented by Ogasawara (1988).||Corrara Granite||||
28703|Mable Downs Granodiorite|22547|6|Mentioned|p17|||Misspelling of Mabel Downs Tonalite.||||||07-MAR-16
28703|Mable Downs Granodiorite|30759|6|Mentioned|p16|||Map of East Kimberley Region||||||
28703|Mable Downs Granodiorite|41977|6|Mentioned|p471|||Misspelling of Mabel?||||||
28703|Mable Downs Granodiorite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
28703|Mable Downs Granodiorite|45047|4|Described|Table 1|||Proterozoic.||||||
69483|MacDougall Bluff Formation|61154|5|Briefly described|p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of the Tollu Group (Bentley Supergroup). Quartz conglomerate with arkosic matrix.  Geological Province: Musgrave Block.||||||
69483|MacDougall Bluff Formation|62989|6|Mentioned|p39|||Of the Tollu Group.  Correlated with Karukali Quartzite.||||||
69483|MacDougall Bluff Formation|65256|5|Briefly described|p14 Fig.10|||Referenced throughout these explanatory notes as MacDougall Formation but in Fig. 10 called MacDougall Bluff Formation. Quartz conglomerate with arkosic matrix.||||||25-MAR-15
81431|MacIntosh Intrusion|70731|6|Mentioned|p271|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. ||||||
26713|Macdougall Formation|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Formation of Tollu Group||||||
26713|Macdougall Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26713|Macdougall Formation|61339|5|Briefly described|Map legend|||Of the Bentley Supergroup. Basal quartz-pebble conglomerate interbedded with cross-bedded arkose and sandstone.||||||
26713|Macdougall Formation|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Tollu Group. Overlain conformably by Mummawarrawarra Basalt. Consists of quartz pebble conglomerate and sandstone.||||||
26713|Macdougall Formation|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Kunmarnara Group, Bentley Supergroup. Age shown as >1078 Ma. Amygdaloidal basalt to andesite metamorphosed to lower amphibolite facies, quartz pebble metaconglomerate, quartzite, phyllite; mafic intrusions.||||||
26713|Macdougall Formation|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Unit in Kunmarnara Group.|||Quartz-pebble conglomerate and sandstone.|
26713|Macdougall Formation|66282|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Has a separately-mapped but un-named foliated unit.||Unit in Kunmarnara Group.|||Quartz-pebble conglomerate and sandstone. Includes an un-named unit of metamorphosed, strongly foliated, quartz-pebble conglomerate, feldspathic sandstone, muscovite quartzite, and phyllite; locally garnetiferous near mafic intrusions.|
26713|Macdougall Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
26713|Macdougall Formation|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1176+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Metasandstone.|
39301|Macedon Member|24368|6|Mentioned|p12|||Contains an oil bearing sandstone reservoir.||||||
39301|Macedon Member|50025|5|Briefly described|p12|Early Cretaceous|Late Jurassic|Forms a basin floor submarine sand fan - hydrocarbon charged.  Overlies the Dingo Claystone.  Geological Province: Exmouth Sub-basin.||||||
39301|Macedon Member|61555|5|Briefly described|p239, 243|Tithonian|Tithonian|Exmouth Sub-basin. Age based on palynology, dinoflagellates: in Pseudoceratium iehiense 4ciia-4ciic subzones of Helby. Youngs to east. Gas reservoir unit.||Of Barrow Group.||Unconformably overlies Dupuy Formation.|Shallow marine sandstone.|20-MAR-12
75593|Macedon Mudstone|61555|6|Mentioned|p234|||BHP Billiton nomenclature. Replaced by [invalid use of] Muiron Member.||||||
75593|Macedon Mudstone|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Dupuy Formation, Dingo Claystone. Is overlain by Lower Barrow Group.||
24368|Madang Tuff Member|23570|4|Described|p236 Appendix 1|||Forms part of the Hardey Formation.  Thickness: up to 130m.||||||
24368|Madang Tuff Member|40369|6|Mentioned|p13|||Mention Plate 2A-2C, Fig.24 as Madang Tuff||||||
24368|Madang Tuff Member|44152|6|Mentioned|p170|||Blight (1985). Similar to Lyre Creek Agglomerate Member.||Hardey Sandstone||||
24368|Madang Tuff Member|72712|6|Mentioned|p8.|Neoarchean|Neoarchean|Blight (1985) recognized this member as part of the Hardey Formation in the Rocklea Anticline but no member-level units are recognised in the Hardey Syncline.|c. 2763 Ma to c. 2745 Ma.|Hardey Formation|||Volcaniclastic rock.|
70466|Maddina Basalt formation|62094|6|Mentioned|p235|Archean|Archean|Informal version of Maddina Formation. Age: 2.78Ga.||||||22-OCT-15
78750|Maddina Sequence|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean|Of Blake (1993). Shown as equivalent to Maddina Formation.||Mount Jope Supersequence.||||24-APR-20
69023|Madfish basalt|60976|6|Mentioned|p12|||Informal name. Feldspar porphyritic basalt. A marker unit. Associated with the Bronzewing fold deposit / Bronzewing anticline. Geological Province: Yilgarn Craton.||||||
69379|Madfish dolerite|60980|5|Briefly described|p142 Fig.2, p144|||Informal name.||||||27-JUN-05
27275|Madley Beds|38898|6|Mentioned|Table 1|||||||||
27275|Madley Beds|45149|2|Defined|p31|Early Cambrian|Early Cambrian|See also Table 1.||||||
27275|Madley Beds|46975|6|Mentioned|p83|||||||||
70745|Madley Formation''|62453|6|Mentioned|p18|||Informal name.||||||
70744|Madley'' Formation|62453|6|Mentioned|p18|||Informal name.||||||
81732|Madoonia syenite''|23584|6|Mentioned|p17|||Geological Province: Yilgarn Craton. Previous name for a quartz monzodiorite to leucogranodiorite. labelled Agdq.||||||22-NOV-19
81732|Madoonia syenite''|71270|5|Briefly described|177913.1.pdf|||Geological province: Yilgarn Craton, West Australian Craton. Nomenclature of Griffin (1989). original name of fine-grained porphyritic tonalite, sample 177913. Sampled 2004, dated 2005.|2663+/-6 Ma igneous crystallisation.|||||22-NOV-19
72754|Madora Formation|61814|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Geological Province: Eucla and Officer Basins.||||||08-FEB-10
70610|Maggie Hays formation|61898|5|Briefly described|p109 Fig. 1|||Informal name.||||||
41459|Maggoty Springs Granite|50437|6|Mentioned|p4.2|||Geological Province: Kimberley Region. Of the Kevins Dam Suite.||||||
33976|Maggoty Springs Monzogranite|22547|3|Fully described|p17||Orosirian|Of the Sally Downs supersuite.||||||14-NOV-06
33976|Maggoty Springs 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
33976|Maggoty Springs Monzogranite|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sally Downs Supersuite.||||||07-NOV-08
75100|Mahogany Creek Granite|64769|6|Mentioned|p31 Tb. 4, p33, p34 Fig. 22, p118|||Light-medium grey and medium-grained granite. WA.||||||21-APR-09
29991|Main Tuff Interval|43064|5|Briefly described|p69|||Informal stratigraphic unit of Bee Gorge Member.||||||
29991|Main Tuff Interval|73022|6|Mentioned|p3 Fig.2, p4 Fig.3|Neoarchean|Neoarchean||2.58 Ga|Bee Gorge Member|||Felsic tuff.|
30535|Malcolm Gneiss|22792|6|Mentioned|p56|||||||||
30535|Malcolm Gneiss|24526|5|Briefly described|p105 Fig. 6, p108|Mesoproterozoic|Mesoproterozoic|Comprises paragneiss units dominated by psammite and quartzite with minor garnet-biotite-sillimanite metapelite; intruded by felsic and mafic orthogneiss.  Cut by dykes of Recherche Granite.  Age: 1500-1190Ma.  Part of the Albany-Fraser Orogen. See also||||||10-APR-08
30535|Malcolm Gneiss|43203|5|Briefly described|Map Legend||Proterozoic|Fraser Complex||||||
30535|Malcolm Gneiss|43498|5|Briefly described|6, 7|||U-Pb age: 1450Ma||||||
30535|Malcolm Gneiss|62381|5|Briefly described|p2 Fig.2, p3 Fig.3, p7-8.|||Age from a poorly defined zircon population from a granitic orthogneiss within Malcolm Gneiss (Myers, 1995).|c.1560 Ma to c.1400 Ma.|Unit in Nornalup Complex.||Cut by dykes of Recherche Granite.|Paragneiss units dominated by psammite and quartzite with minor garnet-biotite-sillimanite pelite, intruded by felsic and mafic orthogneiss.|02-JUL-14
30535|Malcolm Gneiss|62978|5|Briefly described|p181-182|Mesoproterozoic|Mesoproterozoic|Age: ~1560Ma (detrital zircon population). At edge of Albany-Fraser province. Geological Province: Gawler Craton.||||||07-FEB-11
30535|Malcolm Gneiss|63866|5|Briefly described|p183, p190-p191, p193, p198|||Nornalup Complex.|1500-1190 Ma|||Intruded by the Recherche Granite.|Paragneiss units dominated by psammite and quartzite with minor garnet-biotite-sillimanite pelite inruded by felsic and mafic orthogneiss.|
30535|Malcolm Gneiss|64580|4|Described|map legend||Mesoproterozoic|Quartzite, psammite and minor pelite; granitic gneiss, mafic gneiss and granite and pegmatite dykes.||||||15-DEC-08
30535|Malcolm Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p18-19|Calymmian|Calymmian|Of the Albany-Fraser Orogen. Zircon age of 1500-1400 Ma.||||||
30535|Malcolm Gneiss|65487|3|Fully described|p24, 51-52, 54, p56 Fig. 27, p58 Fig. 29|Mesoproterozoic|Mesoproterozoic|Primary constituent of the eastern Nornalup Zone of the Kepa Kurl Booya Province; siliciclastic metasedimentary rocks and orthogneiss: mafic amphibolite schist, quartzofeldspathic gneiss, minor calc-silicate rocks, and c.1330 Ma Recherche Supersuite intrusions (= minimum deposition age). 1560 +/- 40 Ma = maximum deposition age.||||||
30535|Malcolm Gneiss|66256|6|Mentioned|p46 Fig.43a|||Schematic of tectonic evolution of Albany-Fraser Orogen: Proto-Nornalup Zone (includes Malcolm Gneiss) 1345-1320 Ma.||||||
30535|Malcolm Gneiss|67268|5|Briefly described|p8, p15, p16|||Nornalup zone. Protolith approximately 1560 Ma in age and underwent low P high T metamorphism at approximately the same time as the intrusion of the Recherche Supersuite.|||||Siliciclastic meta-sedimentary rocks, orthogneiss, mafic amphibolite schist, quartzofeldspathic gneiss and minor calc-silicate rocks. Muscovite-biotite psammite, quartzites and minor garnet-biotite sillimanite metapelites.|15-JUN-22
30535|Malcolm Gneiss|67581|6|Mentioned|p44 Fig.8|||||||||
30535|Malcolm Gneiss|67722|4|Described|p1-2, p5,12,13,16,17,19,21,26-60,87-101|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.  Age constrains maximum estimate for deposition of sedimentary protoliths. Intruded by pegmatite in shear zones at 1165 +/-5 Ma, marking the end of tectonic activity. Metamorphic and deformation events discussed.|1455+/-16 Ma (SHRIMP) Max depositional age|||Intruded by Recherche Supersuite.|Highly deformed amphibolite facies orthogneiss and paragneiss. Amphibolitic schist, quartzofeldspathic gneiss and minor calc-silicate rocks; arkosic metapsammites and quartzites make up ~half the outcropping Malcolm Gneiss.|
30535|Malcolm Gneiss|68186|6|Mentioned|p26|||Myers (1995). Subsequently renamed Malcolm Metamorphics.||||||
30535|Malcolm Gneiss|68654|6|Mentioned|p3|||Of Myers (1995) and others. Replaced by Malcolm Metamorphics.||||||
30535|Malcolm Gneiss|69252|6|Mentioned|p15-17|||Myers (1995). Subsequently the Malcolm Metamorphics. P-T path illustrated.||||||
30535|Malcolm Gneiss|70023|6|Mentioned|p169|||Geological province: Albany-Fraser Orogen. Superseded. See Malcolm Metamorphics.||||||
30535|Malcolm Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, gneiss|
41116|Malcolm greenstones|24196|6|Mentioned|p8|||Informal name. Referring to greenstones of the Malcolm greenstone belt. Geological Province: Yilgarn Craton.||||||
41116|Malcolm greenstones|60416|5|Briefly described|p7|||Informal name.  Located between the Yilgangi Fault and Mount George Shear Zone.  Mainly felsic volcanic rocks, basalt, shale and dolerite sills; conglomerate in the south.  Correspond largely to the Malcolm greenstone belt of Griffin (1990).||||||15-MAR-05
80617|Mallana Mafic Suite|71803|6|Mentioned|p381||||ca. 2970 -2950 Ma|||||
80890|Mallawa Salt|71870|6|Mentioned|p3|Rhuddanian|Hirnantian|Canning Basin.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.||
81614|Mallawo Salt|69029|6|Mentioned|p319|Late Ordovician|Late Ordovician|Of Canning Basin.||||Overlain by Sahara Formation. Underlain by Nibil Formation.||
81614|Mallawo Salt|69312|6|Mentioned|p3, p24 fig 28|Llandovery|Late Ordovician|Canning Basin. Misspellng of  Mallowa Salt (to which it is correctly referred as on p19). See also  p25 fig 30, p27 fig 34, p28 fig 36.||Carribuddy Group||Overlies the Nibil Formation. Overlain by the Sahara Formation.|Salt.|
81164|Malley Springs Sandstone Member|70315|6|Mentioned|p23|||Kalkarindji Province. 3-5m thick.||Antrim Plateau Volcanics||Overlain by the Mount Close Chert Member.||
39663|Mallowa Formation|24449|5|Briefly described|p741|Llandoverian|Ashgillian|Name used interchangeably with Mallowa Salt.  Geological Province: Canning Basin.||||||
23754|Malu Quartzite|23758|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Incorporated into Malu Formation. Geological Province: Yeneena Basin.||||||
23754|Malu Quartzite|23900|4|Described|p1537 Fig. 2|Proterozoic|Proterozoic|Of the Lamil Group. Overlies the Isdell Formation. Overlain by the Telfer Formation. Geological Province: Paterson orogen.||||||
23754|Malu Quartzite|24194|5|Briefly described|p900 Fig.3|Neoproterozoic|Neoproterozoic|Quartzite, quartz sandstone with minor argillaceous siltstone and mudstone. Parent: Lamil Group. Geological Province: Paterson Orogeny||||||
23754|Malu Quartzite|36551|6|Mentioned|Table 22|||||||||
23754|Malu Quartzite|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23754|Malu Quartzite|37212|6|Mentioned|Table 1|||||||||
23754|Malu Quartzite|37460|4|Described|Table3.VII|||||||||
23754|Malu Quartzite|37707|6|Mentioned|Table I|||||||||
23754|Malu Quartzite|41892|6|Mentioned|Fig.3|||||||||
23754|Malu Quartzite|42730|6|Mentioned|Fig 13, P17|||||||||
23754|Malu Quartzite|43278|4|Described|p644,Fig.2.Fig.3.|Neoproterozoic|Neoproterozoic|of Yeneena Group.||||||
23754|Malu Quartzite|43862|5|Briefly described|Fig.2 p378|||||||||
23754|Malu Quartzite|43867|5|Briefly described|p199,201|||||||||
23754|Malu Quartzite|43868|5|Briefly described|Fig.2 p153,Fig3 p154|||||||||
23754|Malu Quartzite|44139|5|Briefly described|p277-280|Neoproterozoic|Neoproterozoic|Chin et al. (1982). 0-1000 m. Metamorphosed quartz sandstone. Northeastern zone of Yeneena Basin; wedges out to the SW. Conformably overlies Isdell Formation. Overlain by Telfer Formation. Originally called "Core Sandstone" in the Telfer Dome (Blockley 1974).| | ||||05-MAR-18
23754|Malu Quartzite|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
23754|Malu Quartzite|62453|6|Mentioned|p68|||Superseded by Malu Formation. ||||||
77230|Mamut suite|67375|5|Briefly described|p18 Fig.11, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|Yb-depleted. Early Musgrave Orogeny.|1217-1205 Ma.|Unit in Pitjantjatjara Supersuite.|||Thin, NE-trending dykes of very highly-depleted ytterbium granite.|
77230|Mamut suite|67553|5|Briefly described|p19,26,31|Ectasian|Ectasian|Geological province: Musgrave Province, North Australian Craton. Associated with high-pressure melting and low-Yb magmatism (GSWA 184146, 185610 and 187274). Oldest manifestation of the Pitjantjatjara Supersuite in the region.|1217-1205 Ma|Unit of Pitjantjatjara Supersuite.||||
77230|Mamut suite|69091|5|Briefly described|p65|||Of Smithies et al. (2010). Has compositions that are very highly depleted in ytterbium and other heavy rare-earth elements compared with all other granites of Pitjantjatjara Supersuite, with exception of Pirntirri suite. Granites of Pirntirri suite and of Mamut suite are oldest local manifestation of Pitjantjatjara Supersuite.||Pitjantjatjara Supersuite||||
77230|Mamut suite|69729|5|Briefly described|p74-78|||Is also presented variously as Pirntirri-Mamut suite, Mamut-Pirntirri suite and Mumut[sic]-Pirntirri suite. They are collectively described as a regional, compositionally distinctive suite, representing the earliest stages of Musgrave Orogeny magmatism in the Tjuni Purlka Zone (c.1217 Ma) and the Mamutjarra Zone (c.1200 Ma). Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granite dykes and plutons.|
25199|Mandilla conglomerate|30900|5|Briefly described|p69|||||||||
34418|Manganese subgroup|22716|6|Mentioned|table4, p237|Ectasian|Ectasian|Age: 1300 Ma. Part of the Bangemall Basin succession.||||||
72628|Mangaroo Formation|62837|6|Mentioned|Table C|||Misspelt - see Mungaroo Formation.||||||
77745|Mantungula Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|[Formal name is Mantungula Formation].||Unit in Roper Group.||||15-MAR-13
77694|Manubia Sandstone|68298|6|Mentioned|p250 App. 1|||[Misspelling of Munabia Sandstone?]||||||
36841|Manyutup Tonalite Complex|23727|4|Described|11p|Archean|Archean|See also Manyutup Tonalite.||||||07-NOV-08
36841|Manyutup Tonalite Complex|23728|5|Briefly described|Map Legend|Archean|Archean|Underlying unit Annabelle Volcanics. Geological Province: Yilgarn Craton.||||||07-NOV-08
36841|Manyutup Tonalite Complex|69404|6|Mentioned|p10|||Ravensthorpe Terrane. ||||||
83151|Manyutup tonalite|72491|6|Mentioned|p7, 40, 58|||Witt (1999). Ravensthorpe Belt, Youanmi Terrane, Yilgarn Craton.|||||Calc-alkaline magmatic arc complex.|
38665|Maori Queen granitoid|23786|5|Briefly described|p35 Tb. 4|||Informal name.  Geological Province: Yilgarn Craton.||||||
38773|Mara Mamba Iron Formation|23890|5|Briefly described|p10|Archean|Archean|Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
41235|Maraloou-Killara Formation|50226|5|Briefly described|p421 Fig. 4|||Informal grouping of two units, the Maraloou Formation and the Killara Formation, of the Mooloogool Group.  Geological Province: Yerrida Basin.||||||
38774|Maralou Formation|23890|5|Briefly described|p21 Fig.11|||Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
38774|Maralou Formation|65692|5|Briefly described|p55|||Yerrida Basin. Maximum depositional age: detrital zircons.|1843 Ma (Halilovic et al., 2004).|||||
38774|Maralou Formation|68561|5|Briefly described|GLENGARY_GEOLOGYP_LUT.csv||Proterozoic|[Misspelling of Maraloou Formation]|||||Thin-bedded siltstone; Fine-grained limestone; local intercalations of thin amygdaloidal basalt;|
38774|Maralou Formation|69596|5|Briefly described|p9-10, p17|||Yerrida Basin.||Mooloogool Group.|||Finely laminated siltstone and sulfidic shales.|
80211|Mararoa Basalt|71166|6|Mentioned|p14|||Hosts gold reefs.||||||
32638|Marble Bar Jaspilite|45923|14|Not recorded|p111(& 116)||Archean|||||||07-NOV-08
38480|Marda Calc-alkaline suite|36007|14|Not recorded|not recorded|||Name present in title.||||||09-AUG-05
78515|Marda Volcanic Complex|68107|5|Briefly described|p618|Neoarchean|Neoarchean|Eastern Youanmi Terrane.|c.2735 Ma.||||Felsic magmatic and volcanic rocks.|
78515|Marda Volcanic Complex|73596|6|Mentioned|p1165, 1172|Neoarchean|Neoarchean|Southern Cross Domain, Youanmi Terrane.|2732 +/- 3 Ma (Nelson, 2001).||||Andesitic and rhyolitic lava flows and associated pyroclastic rocks (rhyolite ignimbrite, rhyodacite tuff), with minor polymict conglomerate and sandstone.|
25206|Marda andesites and rhyolites|38012|6|Mentioned|p84|||||||||
26722|Mardie Greensand|6876|6|Mentioned|p100 Fig.5.|Early Cretaceous|Early Cretaceous|||||||
26722|Mardie Greensand|12471|5|Briefly described|p474.|Early Cretaceous|Early Cretaceous|This unit's rank (Member) was omitted. Oil and gas shows occurred in this unit during a 1966 seismic survey and subsequently. See Mardie Greensand Member.||||.||24-OCT-14
26722|Mardie Greensand|13615|3|Fully described|p4, p12, p18-20, p35, p102 App. 3|Aptian|Valanginian|Peedamullah Shelf. Commonly <30m thick, maximum thickness is up to 60m. Spores/Pollen Zone and Dinoflagellate zones provided. Rocks in Crackling 1 previously assigned to this unit have been reassigned to the Birdrong Sandstone. Intersected in numerous drillholes. The type section is Mardie 1 drillhole; 145-172m. Contains abundant microfossils which are the basis for its age. Deposited in a low to moderate energy marine shelf and slope. See also p38, p40-p43, p48-p49, p51-p53, p60-63, p65, p68, p71, p73-p74, p83, -85, 87, p118.||Of Winning Group.||Overlies the Birdrong Sandstone transitionally. Unconformably overlies the Flacourt Formation. Overlain by the Muderong Shale.|Fine-grained, glauconititc, well-sorted, pyritic sandstone.|07-FEB-19
26722|Mardie Greensand|23359|6|Mentioned|81|||||||||
26722|Mardie Greensand|23379|4|Described|p161-162,168-170,173|Hauterivian|Valanginian|Used as abbreviated synonym for the preferred Mardie Greensand Member. Of Muderong Shale, Barrow Sub-basin, Carnarvon Basin.||||||22-OCT-14
26722|Mardie Greensand|23726|4|Described|p62|Early Cretaceous|Early Cretaceous|Of Winning Group. Overlain by Muderong Shale. Underlain by Flacourt Formation. Geological Province: Carnarvon Basin.||||||30-APR-09
26722|Mardie Greensand|24084|5|Briefly described|p146 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
26722|Mardie Greensand|24205|5|Briefly described|p242|||Overlain by Muderong Shale.  Geological Province: Northern Carnarvon Basin.||||||
26722|Mardie Greensand|24315|5|Briefly described|p43|Neocomian|Neocomian|Informal - see Mardie Greensand Member. Geological Province: Barrow Sub-Basin.||||||
26722|Mardie Greensand|24331|4|Described|p473, 475|Barremian|Valanginian|See also Mardie Greensand Member. Dark-green to green grey glauconitic, heavily bioturbated siltstone to fine-grained sandstone with interbedded siltstone and shale. Unconformably overlies Barrow Group. Grades up into Muderong Shale. GP: Barrow Sub-basin.||||||21-DEC-04
26722|Mardie Greensand|24351|5|Briefly described|p39, Plate 4 (in pocket)|Early Cretaceous|Early Cretaceous|Geological Province: Exmouth Sub-basin (offshore). Massive and interbedded sands.||||||13-DEC-07
26722|Mardie Greensand|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
26722|Mardie Greensand|33450|6|Mentioned|p10|||||||||
26722|Mardie Greensand|34840|6|Mentioned|p68|||||||||
26722|Mardie Greensand|35144|6|Mentioned|p3|||||||||
26722|Mardie Greensand|38654|6|Mentioned|p786|||||||||
26722|Mardie Greensand|38732|6|Mentioned|p32|||||||||
26722|Mardie Greensand|39486|6|Mentioned|p2092|||See also P2093||||||
26722|Mardie Greensand|39757|6|Mentioned|p1605|||||||||
26722|Mardie Greensand|41170|6|Mentioned|Fig.4|||||||||
26722|Mardie Greensand|41438|6|Mentioned|p109|||||||||
26722|Mardie Greensand|41439|5|Briefly described|p122|||||||||
26722|Mardie Greensand|41440|6|Mentioned|p138|||||||||
26722|Mardie Greensand|41441|6|Mentioned|p153|||||||||
26722|Mardie Greensand|41443|5|Briefly described|p164|||||||||
26722|Mardie Greensand|41444|6|Mentioned|Fig.4|||||||||
26722|Mardie Greensand|41445|6|Mentioned|p198|||||||||
26722|Mardie Greensand|41446|3|Fully described|p205|||||||||
26722|Mardie Greensand|41447|6|Mentioned|Fig.3|||||||||
26722|Mardie Greensand|41709|5|Briefly described|p214|||||||||
26722|Mardie Greensand|41732|6|Mentioned|p541|||||||||
26722|Mardie Greensand|42116|6|Mentioned|p45|||See also Fig.18||||||
26722|Mardie Greensand|42395|6|Mentioned|p80|||||||||
26722|Mardie Greensand|42442|6|Mentioned|p28|||Carnarvon Basin.||||||
26722|Mardie Greensand|42598|4|Described|p97, p40|Aptian|Valanginian|Age: Cretaceous (Valanginian to Aptian)||||||
26722|Mardie Greensand|43564|6|Mentioned|p458|||||||||
26722|Mardie Greensand|43711|6|Mentioned|p22|||||||||
26722|Mardie Greensand|43712|5|Briefly described|p11|||||||||
26722|Mardie Greensand|43722|5|Briefly described|p10-12||Cretaceous|||||||
26722|Mardie Greensand|43724|5|Briefly described|p29|||||||||
26722|Mardie Greensand|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
26722|Mardie Greensand|50085|5|Briefly described|p24 Tb. 6|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
26722|Mardie Greensand|60379|6|Mentioned|p126 fig 3|Early Cretaceous|Early Cretaceous|Dampier sub-basin, Carnarvon Basin||||||
26722|Mardie Greensand|60386|6|Mentioned|p302|Early Cretaceous|Early Cretaceous|Perth Basin, Carnarvon Basin. Deltaic-nearshore-shelf. Shown to include some volcanics? Of same age (in part) as Bunbury Basalt?.||||||
26722|Mardie Greensand|61555|5|Briefly described|p247|||Thin glauconitic shallow marine. Overlain by Muderong Formation.||||||
26722|Mardie Greensand|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin. See also p1374.||||||01-SEP-08
26722|Mardie Greensand|62837|5|Briefly described|Stratigraphic columns|Neocomian|Neocomian|Age: 130-120Ma. Geological Province: Exmouth Sub-basin and Barrow Sub-basin.||||||
26722|Mardie Greensand|63950|5|Briefly described|p336 Fig. 4|Hauterivian|Hauterivian|Underlies Muderong Shale. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
26722|Mardie Greensand|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
26722|Mardie Greensand|64973|4|Described|p503, p504 Fig. 2, p504, p505|Hauterivian|Hauterivian|Of Winning Group. Overlain by Muderong Shale, underlain by Birdrong Sandstone. Geological Province: Carnarvon Basin. Composed of medium-grained glaconitic, wave-rippled and bioturbated sandstone.||||||
26722|Mardie Greensand|64977|4|Described|pp491-501.|Early Cretaceous|Early Cretaceous|So-called throughout this article. Its formal name includes its rank of Member (basal, of Muderong Shale). Regionally extensive marine transgressive unit. Producing oil at Barrow Island from 1968 and offshore Saladin Field from 1993. Thin; c.18 m.||Basal unit in Muderong Shale.||Unconformably overlies Barrow Group.|Dark grey-green glauconitic sandy siltstone, interbedded with dark grey siltstone and shale; strongly bioturbated; with siderite and pyrite as cement and nodules, and late carbonate cement.|
26722|Mardie Greensand|65078|6|Mentioned|p35|||This is an examble of a clastic "basal transgressive sand" - indicating deltaics and general shallow marine geology. Age: Triassic?||||||30-APR-09
26722|Mardie Greensand|66126|5|Briefly described|p203, 213, 219|Early Cretaceous|Early Cretaceous|Carnarvon Basin. Inner and outer shelf deposits. Sedimentary facies nomenclature tabulated. Six core-based lithofacies identified.||||Unconformably overlies Barrow Group. Is overlain by Muderong Shale.|Highly to intensely bioturbated, glauconitic sandstones; thin quartz granule- and pebble-rich horizons, and thick quartz-rich sandstones.|
26722|Mardie Greensand|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
26722|Mardie Greensand|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.||||
26722|Mardie Greensand|69689|5|Briefly described|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||Upper Barrow Group.||Overlies Birdrong Formation. Is overlain by Muderong Shale.||
26722|Mardie Greensand|69692|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||||Overlies Barrow Group. Is overlain by Muderong Formation.||
83271|Mardie Greensand Formation|72447|6|Mentioned|p233, p240|Cretaceous|Cretaceous|Proposed source of Robe River deposits [iron ore; altered ooliths and pisoliths], but probably erroneous. Reflects a marine setting. [Superseded by Mardie Greensand Member].||||||
42338|Mardie Greensand member|24315|6|Mentioned|p45|Neocomian|Neocomian|Informal - see Mardie Greensand Member.||||||
35914|Mardie Greenstone|23355|5|Briefly described|8 Fig.1|Early Cretaceous|Early Cretaceous|||||||
32586|Margaret System|45549|4|Described|p.30-32,37,42,43-49||Precambrian|On many pages. SG51-14, SH512,6.||||||
83074|Maria Basaltic Andesite|73151|6|Mentioned|p10, p12 Tb.3, p16|Neoarchean|Neoarchean|Informal unit within the Maria Mine Formation shown on p5, 13 only as Basaltic Andesite? Source of mafic clasts in conglomerates of the Maria Mine Formation.||Maria Mine Formation|||Basaltic andesite.|
77532|Maria Sequence|66880|6|Mentioned|p26. |Archean|Archean|Kalgoorlie Terrane. Probably correlates with Kambalda Sequence.||||Overlies Vivien Sequence.|Basalt-dominant.|01-NOV-12
40333|Marillana Formation""|24573|6|Mentioned|p669|Middle Miocene|Late Oligocene|Introduced by Kneeshaw et al. (2002)||||||
40334|Marillana Pisolite|24573|6|Mentioned|p673|Middle Miocene|Late Oligocene|Geological Province: central Hamersley Province||||||
40334|Marillana Pisolite|65194|6|Mentioned|p107|||Former name for a channel iron deposit in the Marillana Palaeovalley. Subsequently included in the Marillana Formation with all fluvial sediments in that palaeovalley and tributary systems.||||||
40334|Marillana Pisolite|73574|6|Mentioned|p771 Fig.6|||See also Marillana Formation.||||||
40336|Marillana Pisolite""|24573|6|Mentioned|p669|Middle Miocene|Late Oligocene|Introduced by Stone et al. (2002). Informal name - see Marillana Formation||||||
34561|Marillana pisolite|22814|5|Briefly described|p258|||Equivalent to Robe Pisolite in Western Pilbara. Located in Central Pilbara. Iron ore resource.||||||08-MAR-16
81863|Maringiniup Member|68811|6|Mentioned|p180 tbl 39|Cretaceous|Cretaceous|||Of Leederville Formation.||||15-APR-20
40110|Marinoan "cap dolomite"|24161|5|Briefly described|p13|||Forms the top of the Marinoan glacial strata in the Amadeus Basin and Adelaide Rift Complex.||||||
39247|Marligar Formation|24085|5|Briefly described|p34|Aptian|Neocomian|Overlain by Wangalu Mudstone.||||||
29209|Marlooyanoo Formation|37460|6|Mentioned|p172|||||||||
29209|Marlooyanoo Formation|40089|2|Defined|p57|Mesoproterozoic|Mesoproterozoic|||||||
29209|Marlooyanoo Formation|40354|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
29209|Marlooyanoo Formation|40355|4|Described|p12|||||||||
29209|Marlooyanoo Formation|44142|5|Briefly described|p315 Tb.4-4, p324|||~600m thick shallow marine with pro-grading delta deposits.||Kahrban Subgroup||Overlies Coonabildie Formation conformably. Correlated with Collier Subgroup.|Siltstone, laminated shale; minor arenite, carbonate near top.|
29209|Marlooyanoo Formation|50188|5|Briefly described|p15|||Of the Kahrban Subgroup. Commonly indistinguishable from Coonabildie Formation - therefore the name was abandoned for Coonabildie Formation. Geological Province: Officer Basin.||||||16-JUL-08
40822|Marlooyanoo Formation""|50188|6|Mentioned|p16|||Informal - see Marlooyanoo Formation.||||||16-JUL-08
75377|Marnda Moorn Supersuite|68561|5|Briefly described|GEOCHRON files|||Murchison Domain,Youanmi Terrane. See geochron file 185931.1.pdf|||Includes Muggamurra Suite.|||
75377|Marnda Moorn Supersuite|69583|5|Briefly described|p84; Plates 2, 3|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province.|c.1210 Ma.||Muggamurra Dolerite Suite.|||
75377|Marnda Moorn Supersuite|70140|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province.|c.1210 Ma.||Muggamurra Dolerite Suite.|||
75377|Marnda Moorn Supersuite|70226|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province.|c.1210 Ma.||Mugga Murra Dolerite Suite|||16-DEC-15
75377|Marnda Moorn Supersuite|70794|6|Mentioned|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Gnowangerup--Fraser Dyke Suite, Boyagin Dolerite Suite.|||
75377|Marnda Moorn Supersuite|70796|6|Mentioned|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Part of the Marnda Moorn Large Igneous Province. See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 185931.1.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf.|||Includes the Muggamurra Dolerite Suite and the Boyagin Dolerite Suite.|||
75377|Marnda Moorn Supersuite|70802|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Albany-Fraser Orogen. Of Marnda Moorn Large Igneous Province. Events: Marnda Moorn Supersuite Magmatic Event (1218-1202 Ma). See 2_5m_interpdykel15_lut.csv, 250k_pre_mesozoic_interpgeol_lut.csv.|||Includes Gnowangerup-Fraser Dyke Suite.|||
75377|Marnda Moorn Supersuite|71269|5|Briefly described|500k_interpgeol_lut.csv + geochron files|||Of Marnda Moorn Large igneous Province. Events: Warakurna Supersuite Magmatic Event (1084-1040 Ma); Marnda Moorn Supersuite Magmatic Event (1218-1202 Ma). Contains dyke swarms concentrated around the margins of the Yilgarn Craton, and also some that extend well into the craton interior (Wingate et al., 2005).|||Includes Muggamurra Dolerite Suite.|||
75377|Marnda Moorn Supersuite|71270|5|Briefly described|2_5m_interpdykel15_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||Includes Gnowangerup-Fraser Dyke Suite, Muggamurra Dolerite Suite.|||
75377|Marnda Moorn Supersuite|71271|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province.|1215-1205 Ma.||Muggamurra Dolerite Suite.|||
83192|Marnda Moorn dykes|69412|6|Mentioned|p3|||Yilgarn Craton. Large areal extent, short duration, and chemical composition may be consistent with a mantle plume origin.||||||
83192|Marnda Moorn dykes|70017|6|Mentioned|p223|Mesoproterozoic|Mesoproterozoic|Paleomagnetic pole is close to that of the c.1200 Ma metamorphic rocks of the Albany-Fraser Orogen.|c.1.21 Ga.|||||
83192|Marnda Moorn dykes|73056|6|Mentioned|p297-298, p300 Fig.8|Ectasian|Ectasian|Of the Marnda Moorn Large Igneous Province (LIP).|ca. 1210 Ma|||||
70435|Maroonah marble|61273|5|Briefly described|p85|||Not a formal name - a dimension stone commercially known as DESERT GREEN. An attractive deep-green stone displaying thin black swirling veins and small irregular white blebs.||||||
83152|Marpa Igneous Complex|72491|6|Mentioned|p5 Fig.4|||Burtville Terrane, Yilgarn Craton. Abbreviated to Marpa IC in Fig.4. Mis-spelling of Mapa Igneous Complex.||||||
77176|Marra Mamba BIF|67829|5|Briefly described|p447, p452.|||Hosts in situ, near-surface enriched, goethite-rich ore bodies. Suggestion that abundance of primary Fe-rich carbonate may have buffered this unit from silica leaching is disputed; the relative volumes of M-mplH ore were the result of limited near-surface exposures of this unit. [Formal name is Marra Mamba Iron Formation]. MMIF (p452) probably refers to this unit.||||Is overlain by Wittenoom Formation.|Chert and magnetite (in the ratio of roughly 5:4); minor ferrous carbonates and silicates.|
29963|Marra Mamba Iron-Formation|43056|5|Briefly described|Map Legend|||Mis-spelling of Marra Mamba Iron Formation.||||||03-APR-12
76797|Marra Mamba Iron-formation|64725|5|Briefly described|p58.|||Economically important iron ore host.||Basal unit in Hamersley Group.||Is overlain by Wittenoom Dolomite.||
25211|Marra Mamba Series|38790|6|Mentioned|Table 1|||||||||
33839|Marra Mamba Supersequence|22546|6|Mentioned|374|||Compared with Turee Creek Supersequence.||||||
33839|Marra Mamba Supersequence|22682|5|Briefly described|Fig20,p29|Archean|Archean|2681-2590 Ma. Hamersley Province||||||07-NOV-08
33839|Marra Mamba Supersequence|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean|||||||
70210|Marra Mamba iron Formation|61576|5|Briefly described|p774 Fig. 1|Neoarchean|Neoarchean|Age: 2597+/-5Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
70432|Marymia group|61269|6|Mentioned|p85|||Informal name referring to gold deposits.||||||
33869|Mascotte Sill|22534|6|Mentioned|Fig.5 p10|||Of Black Flag Group.||||||02-NOV-06
30321|Maude Headley Volcanic Member|22547|5|Briefly described|p9|Orosirian|Orosirian|Of the Halls Creek Group. Age: 1857-1848 Ma.||||||14-NOV-06
30321|Maude Headley Volcanic Member|66846|5|Briefly described|p549 Fig.2|Orosirian|Orosirian|||Olympio Formation||Coeval with Butchers Gully Member.|Alkaline volcanic rocks.|
30321|Maude Headley Volcanic Member|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||1850-1860 Ma|Olympio Formation||||
30321|Maude Headley Volcanic Member|69003|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.||Olympio Formation.||||
76773|Maude Headley Volcanics|64731|5|Briefly described|p165|Paleoproterozoic|Paleoproterozoic|Eastern Zone of Halls Creek Orogen. Age from felsic volcanics in the formation.|1857 +/- 5 Ma (Page & Sun 1994).|Of Olympio Formation.||||12-APR-12
74716|Maudobar Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group. Misspelling of Maudoobar Sandstone.||||||
74716|Maudobar Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
74716|Maudobar Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
40783|Maynard Hills quartzites|50128|6|Mentioned|p42|||Informally referring to quartzites of the Maynard Hills greenstone belt. Geological Province: Yilgarn Craton.||||||
70423|Mc Phee Formation|61266|5|Briefly described|p56-57 Fig.1|||Misspelt - see McPhee Formation. Of the Warrawoona Group. Geological Province: Pilbara Craton.||||||12-MAY-06
41117|McAuliffe Syenite|24196|6|Mentioned|p44|||||||||
41118|McAuliffe Well syenite|24196|5|Briefly described|p70|Archean|Archean|Age: 2651 +/- 5 Ma (U-Pb: Nelson, 1997). Geological Province: East Malcolm sub-domain, Yilgarn Craton.||||||07-NOV-08
40112|McFadden Formation Equivalent|24161|6|Mentioned|p38|||See McFadden Formation equivalent. Geological Province: Officer Basin.||||||
40111|McFadden Formation equivalent|24161|4|Described|p9 Fig.6, p16|Neoproterozoic|Neoproterozoic|Unconformably and disconformably overlies the Wahlgu Formation. Unconformably overlain by the Table Hill Volcanics. Previously interpreted as the Babbagoola Formation. Geological Province: Officer Basin.||||||
70746|McFadden Formation''|62453|6|Mentioned|p48|||Informal Name.||||||
25220|McFadden Sandstone|33849|4|Described|p126|||||||||
25220|McFadden Sandstone|35596|6|Mentioned|p10|||||||||
25220|McFadden Sandstone|36551|6|Mentioned|p101|||||||||
25220|McFadden Sandstone|37020|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25220|McFadden Sandstone|37022|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25220|McFadden Sandstone|37023|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25220|McFadden Sandstone|37212|5|Briefly described|p15|||||||||
25220|McFadden Sandstone|37214|3|Fully described|p8|||||||||22-DEC-09
25220|McFadden Sandstone|37460|5|Briefly described|p170|||||||||
25220|McFadden Sandstone|37707|6|Mentioned|p16|||||||||
25220|McFadden Sandstone|40089|2|Defined|p54|Mesoproterozoic|Mesoproterozoic|||||||
25220|McFadden Sandstone|43492|6|Mentioned|9|||||||||
25220|McFadden Sandstone|45149|6|Mentioned|p20|||||||||
70747|McFadden Sandstone''|62453|6|Mentioned|p60|||Informal name.||||||
83715|McFarlane's Basalt|70275|6|Mentioned|p471, 480|||The lowermost stratigraphic unit in the Mt. Keith area, Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||Is overlain by Mount Keith Dacite.||
76802|McGrath Formation|64725|5|Briefly described|p64.|Paleoproterozoic|Paleoproterozoic|Ashburton Province. Clastic and carbonate rocks, host to Mount Olympus orogenic gold deposit.|<2455 Ma.|||||
26730|McHale Granodiorite|22440|5|Briefly described|p4|Orosirian|Orosirian|Age: 1824 +/- 3Ma.||||||14-NOV-06
26730|McHale Granodiorite|22547|5|Briefly described|p22|Orosirian|Orosirian|In the Lamboo Complex. Age: 1827 +/- 3 Ma. Overlain by Texas Downs Formation.||||||14-NOV-06
26730|McHale Granodiorite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1835-1805 Ma.||||||07-NOV-08
26730|McHale Granodiorite|23621|6|Mentioned|p54|||||||||
26730|McHale Granodiorite|24173|5|Briefly described|p18, 23|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Overlain unconformably by Red Rock and Texas Downs Formation in Turkey Creek. Age: c.1827Ma||||||07-NOV-08
26730|McHale Granodiorite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
26730|McHale Granodiorite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  In the Bow River batholith.  Age: 1835-1805Ma.||||||07-NOV-08
26730|McHale Granodiorite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26730|McHale Granodiorite|32728|6|Mentioned|Table 4|||||||||
26730|McHale Granodiorite|36885|4|Described|p175|||||||||
26730|McHale Granodiorite|41977|6|Mentioned|p471|||||||||
26730|McHale Granodiorite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
26730|McHale Granodiorite|44155|4|Described|p242 Tb.3-5, p248 Tb.3-8|||East Kimberley. Appears as McHales Granodiorite in Tb.3-8. Probably comagmatic with Bow River Granite.|1850 Ma.|Lamboo Complex||Intrudes Olympio Formation, Whitewater Volcanics, Halls Creek Group. Overlain by Red Rock Beds unconformably.|Biotite and muscovite granodiorite and monzogranite; some hornblende granodiorite.|
26730|McHale Granodiorite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
26730|McHale Granodiorite|45047|4|Described|p13|||See also p27. Age:  c.1850 my.||||||14-NOV-06
26730|McHale Granodiorite|45048|6|Mentioned|p67|||Carpentarian or Lower Proterozoic||||||
26730|McHale Granodiorite|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: 1827 +/- 3Ma (Shrimp).||||||07-NOV-08
26730|McHale Granodiorite|63866|5|Briefly described|p132|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1827 Ma|Sally Downs Supersuite||Unconformably overlain by the Kimberley Group, Red Rock Formation and the Texas Downs Formation.||
26730|McHale Granodiorite|65413|4|Described|pp104-109.|Paleoproterozoic|Paleoproterozoic|Of Dow and Gemuts (1969). Part of the Sally Downs Batholith. Undeformed to weakly deformed, but widespread alteration and other evidence of hydrothermal activity; contrasts with coeval Mabel Downs Tonalite. Alteration is described in detail. Cut by magmatic-hydrothermal breccia dykes which are decribed in detail.|1827 +/- 3 Ma (SHRIMP: Page 1994).|Unit in Lamboo Complex.||Is unconformably overlain by Red Rock Formation.|Coarse-grained, equigranular, leucocratic tonalite, diorite to granodiorite.|
26730|McHale Granodiorite|65417|6|Mentioned|p156.|||||||||
26730|McHale Granodiorite|68078|6|Mentioned|p24|||||||Unconformably overlain by Texas Downs Formation||
26730|McHale Granodiorite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data migrated from OZCHRON1. Original comment: 'This igneous crystallisation age for the granite is based on 20 of the 43 analyses. About half of the other data are discordant and rejected. A few inherited xenocrysts are 1850 Ma and ~1875 Ma.'|Crystallisation age 1827+/-3 Ma U/Pb SHRIMP|Mabel Downs Suite|||Medium- to coarse grained, equigranular biotite-hornblende tonalite and biotite granodiorite; extensive magmatic brecciation and associated alteration.|03-AUG-15
26730|McHale Granodiorite|69165|6|Mentioned|GA_geochron.csv||||1827 Ma|||||
26730|McHale 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.|1827-1827 Ma (Isotopic)|Unit of Mabel Downs Suite.|||Medium- to coarse grained, equigranular biotite-hornblende tonalite and biotite granodiorite; extensive magmatic brecciation and associated alteration|
26730|McHale Granodiorite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1827 Ma|Mabel Downs Suite|||Medium-coarse grained equigranular biotite-hornblende tonalite and biotite granodiorite; extensive magmatic brecciation and associated alteration.|
26730|McHale 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). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1827+\-3 Ma (isotopic)|Unit of Mabel Downs Suite.|||Medium- to coarse grained, equigranular biotite-hornblende tonalite and biotite granodiorite; extensive magmatic brecciation and associated alteration|
26730|McHale Granodiorite|72437|5|Briefly described|p96|||Whole rock analyses are provided.||Mabel Downs Suite|||Foliated biotite monzogranite.|
79542|McIntosh Intrusion|68078|6|Mentioned|p23|||||||||
79542|McIntosh Intrusion|69003|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Intrudes Central and E zones of the Lamboo Province.|||||Layered mafic-ultramafic intrusion.|
79542|McIntosh Intrusion|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Grouped with Springvale and Wilagee intrusions.|||||Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, gabbronorite, magnetite gabbro, magnetite-olivine gabbro, leucogabbro, leucogabbronorite, and anorthosite.|21-NOV-19
79542|McIntosh Intrusion|71873|6|Mentioned|p426|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province.||||||
35387|McIntosh Sill|23205|6|Mentioned|p42|||Unknown State.||||||
31130|McIntosh mafics|43484|6|Mentioned|11-12|||||||||
83157|McLeod Member|72493|5|Briefly described|p30|||Hamersley Basin.||Marra Mamba Iron Formation.||Overlies Nammuldi Member. Is overlain by Mount Newman Member.|Shale.|
41368|McNamara Hill adamellite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Kulgera Suite.||||||
78762|McPhee Chert|62427|6|Mentioned|p17|||In the Marble Bar Greenstone Belt. See references for McPhee Formation, same page.||||Correlated with Razorback Chert.||12-MAR-14
39747|McPhees Hill pegmatite|24193|5|Briefly described|p876|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
25222|McRae Shale Formation|31931|6|Mentioned|p82|||||||||
25222|McRae Shale Formation|69745|6|Mentioned|p277, 284|||Mount Wall area, Hamersley Province. See also references to Mount McRae Formation (p272-273, 287) and Mount McRae Shale (p278-279, 281-282, 290).||||Is overlain by Dales Gorge Member.||
38542|McRae shale|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
75102|Meckering Granite|64769|6|Mentioned|p31 Tb. 4, p33|||Light-medium grey and medium-grained granite. WA.||||||21-APR-09
82334|Medagone Formation|72499|5|Briefly described|p91 App.3.5.||Late Jurassic|Shown as top unit in Roebuck Bay 1. [original well completion report E.T. Kempin, West Australian Petroleum (1956), p3 +composite well log p32, appears to refer to a ?Lower Cretaceous Medalagong Formation 30ft to 500 ft. Sandstone. An attached (p31) Well index sheet revised Feb 1960 and Feb 1969 refers to this interval as Broome Sandstone]||||Shown as overlying Jarlemai Siltstone.||
77190|Median Sandstone Member|44139|6|Mentioned|p281, Table 3-15|Proterozoic|Proterozoic|Of Upper Malu Formation. Informal name (of Turner 1983 PhD thesis). Now included in Telfer Formation.| | ||||10-SEP-12
77178|Median sandstone|23758|6|Mentioned|p9|||Informal mine sequence unit of the Telfer Member.||||||
25225|Medusa Beds""|41839|6|Mentioned|p33|||||||||
25225|Medusa Beds""|42442|6|Mentioned|p13|||Superseded by Tanmurra Formation||||||
38716|Meeberrie Gneisses|24448|5|Briefly described|p158|Archean|Archean|Not intended as a formal name - see Meeberrie Gneiss.  Age: 3357 +/-70Ma (U-Pb).  Geological Province: Yilgarn Craton.||||||07-NOV-08
38715|Meeberrie banded gneiss|24448|5|Briefly described|p158|Archean|Archean|Informal - see Meeberrie Gneiss.  Age: 3750-3500Ma (U-Pb).  Geological Province: Yilgarn Craton.||||||07-NOV-08
23784|Meeberrie gneiss|24448|5|Briefly described|p158|Archean|Archean|Informal - see Meeberrie Gneiss.  Age: 3620Ma (Compston et al 1982).  Geological Province: Yilgarn Craton.||||||07-NOV-08
23784|Meeberrie gneiss|40101|5|Briefly described|p156|||||||||
23784|Meeberrie gneiss|40588|6|Mentioned|Fig.1|||||||||
23784|Meeberrie gneiss|40661|6|Mentioned|p93|||||||||
23784|Meeberrie gneiss|41261|6|Mentioned|p5|||||||||
23784|Meeberrie gneiss|41331|4|Described|p300|||||||||
23784|Meeberrie gneiss|41332|6|Mentioned|p311|||||||||
23784|Meeberrie gneiss|41333|5|Briefly described|p325|||||||||
23784|Meeberrie gneiss|41334|6|Mentioned|p343|||||||||
23784|Meeberrie gneiss|41942|5|Briefly described|p51|||||||||
23784|Meeberrie gneiss|60694|5|Briefly described|p253, p273|Archean|Archean|Informal name.  A complex layered rock containing dismembered enclaves of the Manfred Complex.  Age: ~3730+/-6Ma (zircon).   Geological Province: Narryer Terrane/Yilgarn Craton.||||||07-NOV-08
23784|Meeberrie gneiss|62842|5|Briefly described|p203|Archean|Archean|Of Myers and Williams (1985). Informal - see Meeberrie Gneiss. Oldest identified quartzofeldspathic rocks at Mount Narryer.||||||07-NOV-08
23784|Meeberrie gneiss|66583|5|Briefly described|p803,806,818|Paleoarchean|Paleoarchean|Geological province: Yilgarn Craton. Of the Narryer Gneiss Complex. [Also referred to as granitic gneiss on p803]. Contains various lithological associations derived from monzogranties with zircon U-Pb ages of 3.68-3.60 Ga (Myers and Williams 1985; Kinny et al. 1988; Myers 1988b; Myers et al. 1990; Nutman et al. 1991, 1993). Maximum zircon U-Pb age of 3.73 Ga (Nutman et al. 1991; Kinny and Nutman 1996). Intruded by monzo- or syenogranitic magmas at 3.38-3.35 Ga (Dugel Gneiss protolith; see p806 for references). Contain inclusions of 3.73 Ga Manfred Complex meta-anorthosites, -gabbros and -ultramafic rocks (Myers and Williams 1985; Kinny et al. 1988; Myers 1988a). Contains 3.30-3.28 Ga zircons, interpreted to reflect metamorphism caused by granties emplacement.||||||
23784|Meeberrie gneiss|70332|6|Mentioned|p78|||Mentioned in connection with the need for a contaminating component, similar to this unit, to account for hydrous nature of Narndee Igneous Complex.||||||
23784|Meeberrie gneiss|70500|6|Mentioned|p125-127, 130-135, 139-142|Eoarchean|Eoarchean|Narryer Terrane, Yilgarn Craton. SHRIMP U-Pb and Lu-Hf isotope results tabulated. Appears formally as Meeberrie Gneiss on p141.|3731 +/- 4 Ma (Nutman et al., 1993).|||||
81334|Meekatherra Formation|70030|4|Described|p190,192,207|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton. [Misspelt: Should be Meekatharra Formation as per p192]. Thickness: 2.5km. End of sedimentation coincides with ca. 2760 Ma felsic magmatism, marking likely start of Greensleeves Formation deposition.||Unit of Polelle Group.|Includes Stockyard Basalt.|Conformably overlain by Greensleeves Formation. Conformably underlain by Coodardy Formation.|Tholeiitic basalt, komatiitic basalt, komatiite, felsic volcaniclastic rocks.|08-AUG-19
78503|Meeline Mafic-Ultramafic Suite|68110|6|Mentioned|p673, p674 Fig.2|||Variation on Meeline Suite (p686).||||||10-OCT-14
83160|Meeline suite|72494|5|Briefly described|p28|||Yilgarn Craton. Comprises 38,000 km3 of emplaced intrusions.|c.2815 Ma.||||Anhydrous tholeiitic magma intrusions.|
68967|Meenthena Carbonate Member|24533|5|Briefly described|p11|Archean|Archean|Of the Tumbiana Formation (Fortescue Group).||||||07-NOV-08
70226|Melanganee Formation|24410|6|Mentioned|p30|Quaternary|Quaternary|Dune sands used in cement manufacture,||||||
31101|Melita Complex|23786|5|Briefly described|p18 Fig. 10|||Structural term. Geological Province: Yilgarn Craton||||||
31101|Melita Complex|24196|5|Briefly described|p8|||Geological Province: Yilgarn Craton. Comprises of rhyolitic to dacitic rocks interlayered with pillow basalts and mafic hyaloclastites (Brown et al., 2001).||||||
31101|Melita Complex|24494|5|Briefly described|p14|Archean|Archean|Age: 2683 +/- 3Ma (U-Pb; Brown et al., 2002). Comprises of rhyolitic to dacite lavas and volcaniclastic rocks interlayered with pillow basalts and mafic hyaloclastites.||||||07-NOV-08
31101|Melita Complex|43478|6|Mentioned|p18|||||||||
31101|Melita Complex|63980|4|Described|pp66-70, p73,63.|Archean|Archean|Gindalbie Terrane. 25 km SSE of Leonora. Over 3 km thick. Mafic-dominated units lie below felsic-dominated units. Rhyolites are highly enriched in incompatible elements and are distinctive in the Eastern Goldfields Superterrane.|2683 +/- 3 Ma SHRIMP zircon (Brown 2002).||||Tholeiitic basalt and basaltic andesite lavas, pillowed basalts, mafic hyaloclastite, porphyritic quartz-feldspar rhyolite, rhyolite breccia, felsic and mafic volcanogenic sandstone, chert, dolerite and gabbro sills.|26-SEP-14
31101|Melita Complex|65264|5|Briefly described|p9|||Geological province: Ginbaldie terrane. Bimodal package containing rhyolitic to dacitic lavas and volcaniclastic rocks interlayered with pillow basalts and mafic hyaloclastics.||||||07-FEB-11
31101|Melita Complex|66880|5|Briefly described|p9. |Archean|Archean|Very similar age to rhyolite from Jeedamya Complex to the south.|2683 +/- 3 Ma (Brown et al. 2002).||||Includes rhyolites.|
31101|Melita Complex|68109|6|Mentioned|p660|Neoarchean|Neoarchean|Gindalbie Terrane.|c.2690 - 2680 Ma.||||Bimodal rhyolite-basalt and felsic calc-alkaline volcanic complex.|08-OCT-14
31101|Melita Complex|73391|6|Mentioned|p286|||Gindalbie Terrane. Geochemical similarities with rhyolites in the Kalgoorlie Terrane, and lithological similarities, cast doubt on the Mount Monger Fault as a terrane boundary.||||||
38654|Melita complex|23786|6|Mentioned|p22|||Informal name.  Geological Province: Yilgarn Craton.||||||
38654|Melita complex|24196|6|Mentioned|p8, p42, p44|||Informal - see Melita Complex.||||||
38654|Melita complex|24494|6|Mentioned|p23 Tb.2|||Informal - see Melita Complex.||||||
38650|Melita rhyolite|23786|6|Mentioned|p12|||Not intended as a formal name. Geological Province: Yilgarn Craton||||||
40774|Melita volcanic complex|24494|6|Mentioned|p22|||Informal - see Melita Complex.||||||
40774|Melita volcanic complex|69631|5|Briefly described|p48|Neoarchean|Neoarchean|Melita area. Likely that this will be assigned to the Melita Formation.|c.2683 Ma (SHRIMP U-Pb zircon: Brown et al., 2002)||||A bimodal succession with coeval effusive submarine volcanism and voluminous (effusive, shallow intrusive and explosive) rhyolite volcanism in a shallow-subaqueous setting.|
82134|Melligo-Para-Frozier Sandstone|72497|6|Mentioned|p3 Fig.2.|Aptian|Barremian|[Probably a combination of Melligo Sandstone, Parda Formation, Frezier Sandstone sedimentary package] 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.||||Laterally equivalent to Samuel Formation.||
75992|Mellinjerrie Formation|65382|6|Mentioned|p717 App. 2|Frasnian|Frasnian|Canning Basin. 380 Ma.||||||
33224|Merlinleigh sandstone|44657|14|Not recorded|p.3|||(sandstone).||||||
28110|Merougil Conglomerate|23595|6|Mentioned|p18|||||||||
28110|Merougil Conglomerate|23786|5|Briefly described|p28|Archean|Archean|Age: 2664+/-6Ma. Maximum Thickness: 1400m. Geological Province: Eastern Goldfields Province.||||||07-NOV-08
28110|Merougil Conglomerate|42221|4|Described|p11|||||||||
28110|Merougil Conglomerate|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
28110|Merougil Conglomerate|43101|6|Mentioned|p23|||||||||
28110|Merougil Conglomerate|43162|6|Mentioned|5|||||||||
28110|Merougil Conglomerate|43280|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
28110|Merougil Conglomerate|43496|6|Mentioned|6,15|||Ages: 2680+/-21Ma and 2684+/-6Ma||||||
28110|Merougil Conglomerate|43838|6|Mentioned|p3, 7||Archean|Known to occur in the Yilgarn Craton.||||||12-JUL-16
28110|Merougil Conglomerate|50421|4|Described|p285||Archean|Age: <2655 Ma. Fluvial palaeochannel and bar system. Unconformably overlies Black Flag Group. One of the uppermost units of the Kalgoorlie Terrane.||||||07-NOV-08
28110|Merougil Conglomerate|60076|5|Briefly described|p13, p27|||Along with the Karrawang Formation these are the uppermost of the Kalgoorlie greenstones, comprising rudaceous and arenaceous sedimentary rocks.  See also Merougil conglomerate.||||||13-APR-05
28110|Merougil Conglomerate|60555|5|Briefly described|p2 Fig. 1, p4 Tb. 1, p6 Fig. 3, p8 Tb. 2|Archean|Archean|Age: <2671+/-3 and <2664+/-6Ma. Thickness: 1400m. Polymictic clast and matrix conglomerates interbedded with coarse-grained, cross-bedded, graded sandstone and pebbly conglomerate. Alluvial to fluvial then proximal to medial braid plain.||||||07-NOV-08
28110|Merougil Conglomerate|60627|5|Briefly described|p65 Tb.1|||Polymictic conglomerate, immature sandstone with coarse trough cross beds, graded beds.||||||
28110|Merougil Conglomerate|61144|6|Mentioned|p24 Fig. 28|||In the Kalgoorlie area.||||||
28110|Merougil Conglomerate|64340|6|Mentioned|p2 Fig. 1, p8 Tb. 1|||||||||
28110|Merougil Conglomerate|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Polymictic conglomerate with cross beds and graded beds||||||
28110|Merougil Conglomerate|65260|6|Mentioned|p6 Tb.1|||<2674 Ma.||||||
28110|Merougil Conglomerate|65834|6|Mentioned|p7|||Kambalda Domain, Kalgoorlie Terrane.|||||Polymictic conglomerate; immature sandstone. Coarse trough cross-beds, graded beds.|
28110|Merougil Conglomerate|67198|5|Briefly described|p114, p115, p118 Fig.52, p122, p131|||Now defined as part of the Merougil Sequence. Deposited during a phase of extension and plutonism that formed the Late Basins. Age derived from both U/Pb dating and regional constraints.|2660-2650 Ma|||Disconformably overlies Black Flag Group|Conglomerate and sandstones.|11-SEP-17
28110|Merougil Conglomerate|68289|5|Briefly described|p16-p17|||See also Merougil Formation. Crops out beside the Goldfields Highway. In contact with the Black Flag Group although the nature of this relationship is not made clear (only described as "sharp").||||Equivalent to the Navajo Sandstone.|Coarse-grained, quartz-rich sandstone and conglomerate.|
28110|Merougil Conglomerate|73391|6|Mentioned|p30 Fig.2.5, 236|||Kambalda area.|||||Fluviatile metasedimentary rocks.|
73921|Merougil Group|50548|4|Described|p1174, p1175 Fig.1||Archean|Age: 2664+/-6 Ma. Unconformably overlies Black Flag Group. River sediments.||||||07-FEB-11
73921|Merougil Group|65834|6|Mentioned|p26|||Kalgoorlie Terrane.||||||
73921|Merougil Group|67020|5|Briefly described|p660.|Archean|Archean|||||Unconformably overlies Black Flag Group.|Polymictic sedimentary rocks.|13-JUN-13
73921|Merougil Group|69404|6|Mentioned|p4|Neoarchean|Neoarchean|Kalgoorlie Terrane. |c.2670-2658 Ma|||||
73921|Merougil Group|69583|5|Briefly described|p39|||Correlation based on zircon age ranges and dominance of volcanic-derived quartz grains.||||Correlated with Scotty Creek Formation and Jones Creek Conglomerate.||
73921|Merougil Group|70087|6|Mentioned|p215|Archean|Archean||2670-2658 Ma.|||||
73921|Merougil Group|72049|5|Briefly described|p256, p259-p260|||Informally subdivided into Early and Late components, includes all units in these subdivisions.||||||
73921|Merougil Group|72057|5|Briefly described|p237-238,242|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||||Underlain by Black Flag Group.||
73921|Merougil Group|73391|6|Mentioned|p236|||Squire et al. (2010).||||Correlated with Merougil Conglomerate and Navajo Sandstone.||
41119|Merougil Sandstone|24196|5|Briefly described|p47 Fig.5||Archean|Age: <2671 +/- 3 Ma. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||07-NOV-08
41119|Merougil Sandstone|63637|6|Mentioned|p4 Fig. 1.1|||Geological province:Eastern Goldfields Province. Sedimentary unit.||||||17-OCT-07
41119|Merougil Sandstone|64633|6|Mentioned|p6 Fig.4.|||Kalgoorlie Terrane.|<2664 +/- 6 Ma (Krapez et al. 2000).|||||
41119|Merougil Sandstone|65264|5|Briefly described|p21|||Max. thickness: 300m. Outcrops on LAKE LEFROY map sheet. Consists of immature sedimentary rocks - mainly crossbedded, pebbly sandstones, but include high proportions of conglomerate and siltstone.||||||07-FEB-11
41119|Merougil Sandstone|66880|6|Mentioned|p8 Fig.2. |Archean|Archean|Formal name is Merougil Conglomerate.|c.2670 Ma.|||||
41119|Merougil Sandstone|71212|4|Described|p241|Neoarchean|Neoarchean|Kalgoorlie region. Deposited in a sub-aerial (fluvial) braided plain environment. |Approx. 2660 Ma.|||Unconformably overlies the Black Flag Formation.|Upwards fining succession of quartzofeldspathic conglomerate and sandstone.|
41119|Merougil Sandstone|72049|5|Briefly described|p254, p256-p257, p259, p272|||SHIRMP and LAICPMS analytical techniques and results are discussed in detail. At St Ives the unit is >1630m thick (Krapez et al., 2008. Mistakenly referred to as the Merougil Formation on p272.||Early Merougil Group|||Sandstone dominated by large grains of volcanic quartz and minor feldspar fragments.|
77533|Merougil Sequence|63981|6|Mentioned|p91, p93 Fig.3, |Archean|Archean|One of four unconformity-bounded second-order sequences recognised in the Kalgoorlie Terrane. There is a formally-named unit, the Merougil Conglomerate.||||||
77533|Merougil Sequence|66880|5|Briefly described|p7, p28. |Archean|Archean|Part of the uppermost of three lithostratigraphic divisions in the Kambalda Domain.|Detrital zircons 2664 +/- 6 Ma.||||Siliciclastic sedimentary rocks.|
77533|Merougil Sequence|67198|5|Briefly described|p81-83, p112 Fig.48, p114, p120|||Fluvial bar and channel system deposits.Timing of gold mineralisation in the St Ives goldfield is younger than this Sequence.|<2660 Ma (maximum depositional age).|||Unconformably overlies Kalgoorlie Sequence.|Upward-fining successions of conglomerates and sandstones.|11-SEP-17
77533|Merougil Sequence|68109|5|Briefly described|p660|Neoarchean|Neoarchean|Product of a cycle of felsic pyroclastic eruptions and emplacement of high-Ca granites.|> 2660 Ma|||Unconformably overlies the Kambalda and Kalgoorlie Sequences.||08-OCT-14
77533|Merougil Sequence|73391|6|Mentioned|Appendices.|||Barley et al. (2002). Regional stratigraphic correlation chart of other workers.||||||
34372|Merougil Supersequence|22682|5|Briefly described|p15||Archean|||||||07-NOV-08
34372|Merougil Supersequence|66936|5|Briefly described|pp136-141. |Archean|Archean|Kalgoorlie Terrane. Fining-upwards units typical of gravelly river systems.||||Unconformably overlies Kalgoorlie Sequence.|Conglomerates, clast supported; sandstones, medium- to coarse-grained, subrounded to angular grains of quartz, sericitised feldspar and rock fragments.|
34372|Merougil Supersequence|66937|6|Mentioned|p155. |Archean|Archean|Kalgoorlie Terrane.||||||
34372|Merougil Supersequence|66938|5|Briefly described|p186. |Archean|Archean|Autocyclic controls on stratigraphic patterns are identified by lateral switching between channel and bar deposits within sedimentation units. The first stratigraphic response to collision of the Eastern Goldfields Superterrane onto the Yilgarn continent.||||||
41086|Merougil conglomerate|24139|5|Briefly described|p239 Table 1|||Geological Province: Kambalda Domain.||||||
41086|Merougil conglomerate|60076|5|Briefly described|p12 Tb. 2|||Informal - see Merougil Conglomerate.  Thick, mostly pebbly sandstone, sandstone and siltstone.  Max. thickness: 2300m.  Geological Province: Kambalda domain.||||||
77564|Merougil-Navajo Supersequence|66938|6|Mentioned|p187. |Archean|Archean|This name is presumably meant to be shorthand for "Merougil and Navajo Supersequences" (q.v.); the apparent interchangeability in this article of the terms Supersequence and basin adds to the confusion. An axial (fluvial environment) system, with transport to the south or southeast, implying north to south paleoslopes. Depositional facies are characteristic of high-discharge bedload draining areas of high relief. ||||||
28747|Mertondale "granite"|30440|6|Mentioned|p5|||||||||
69751|Michael Hills gabbro|44109|6|Mentioned|p55|Mesoproterozoic|Mesoproterozoic|Informal name referring to the gabbro of the Michael Hills gabbro intrusion. Within the Giles Complex.  See also p106 Fig. 122. ||||||
69751|Michael Hills gabbro|61340|6|Mentioned|Map legend|||Stated to include the Latitude Hill Gabbro/Pyroxenite Intrusion (as a segment).||||||
69751|Michael Hills gabbro|69655|6|Mentioned|p16|||||||||
69755|Michael Hills gabbro intrusion|44109|5|Briefly described|p9, p55|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex.  Gabbro, containing locally abundant thin pyroxenite layers. Tectonic segment of  Michael Hills intrusion. ||||||
69755|Michael Hills gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: <8000m.||||||21-SEP-05
78331|Michael Hills intrusion|65135|5|Briefly described|p14, p17|||Informal name. Gabbroic. Of the layered Giles intrusions. Cross-cut by Gairdner dykes.||||||
78331|Michael Hills intrusion|68996|5|Briefly described|p45-47, 48, 50, 51, 57,59,62,63,64,65,68|Mesoproterozoic|Mesoproterozoic|Part of G1 group. Along with Latitude Hills intrusion, characterised by very strong aeromagnetic anomalies.||Giles Suite.||||
69768|Michael Hills layered intrusion|61339|6|Mentioned|Map legend|||Informal name.||||||
39719|Middle Creek formation|23936|6|Mentioned|Fig.19a|||Geological Province: Pilbara Craton.||||||
39719|Middle Creek formation|24188|4|Described|p789, 795|Archean|Archean|Informal name. Age: ~3280 Ma, (SHRIMP U-Pb zircon). Geological Province: Pilbara Craton||||||07-NOV-08
28751|Middle Lamboo Complex|48931|4|Described|p20|||||||||
77191|Middle Vale Shale|44139|6|Mentioned|p281, Table 3-15|||Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation.| | ||||10-SEP-12
77179|Middle Vale siltstone|23758|6|Mentioned|p9|||Informal mine sequence unit of the Telfer Member.||||||
32790|Middle unit|44230|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
32790|Middle unit|44231|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
25237|Milligan Beds|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
25237|Milligan Beds|44994|6|Mentioned|p14|||Correlation. Fig.6||||||
34328|Millina Formation|22717|6|Mentioned|P5||Archean|||||||07-NOV-08
40066|Millindina Complex|23936|5|Briefly described|Tb.1|Archean|Archean|Age: c.2.925Ga. Geological Province: Pilbara Craton. Misspelt - see Millindinna Complex.||||||07-NOV-08
37090|Millindina Complex""|23743|5|Briefly described|p9|||Superseded - now named Millindinna Intrusion.||||||
73601|Millindinnah Complex|63441|6|Mentioned|p12 Tb. 2|Archean|Archean|Misspelt - name is Millindinna.  Millindinna Complex has been superseded by Millindinna Intrusion.||||||07-FEB-11
74717|Millindinnah Intrusion|64580|4|Described|map legend||Mesoarchean|Of the Langenbeck Suite.  Misspelling of Millindinna Intrusion. Gabbro, pyroxenite, and peridotite; metamorphosed.||||||17-DEC-08
74717|Millindinnah Intrusion|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2950 Ma|Unit of Lagenbeck Suite.|||Gabbro, pyroxenite, and peridotite; metamorphosed|
80079|Millinjierie Formation|69312|6|Mentioned|p15|||Canning Basin. [ Misspelling of Mellinjerie Limestone]||||||11-FEB-20
70372|Milliwindi dolerite|23328|4|Described|1031-1038|||SHRIMP U-Pb zircon age 513+/-12 Ma. Intrusive feeder for Antrim Plateau Volcanics. At least 200 km long, although discontinuous now. Lith description, geochem analysis given.||||||22-SEP-17
70372|Milliwindi dolerite|61716|5|Briefly described|p650|Cambrian|Cambrian|Informal name.  Dyke formation - geochemically identical to basalts of the Antrim Plateau Volcanics.  Age: 513+/-12Ma.||||||19-MAY-06
70372|Milliwindi dolerite|62557|5|Briefly described|p461|Middle Cambrian|Middle Cambrian|Of the Kalkarindji continental flood basalt province. SHRIMP U/Pb zircon age 513+/-13 Ma.||||||13-OCT-09
70372|Milliwindi dolerite|65337|6|Mentioned|p94.|||Shown in inverted commas to emphasise informal status.||Unit in Kalkarindji Volcanic Group.||||
23792|Millstream Dolomite|38776|2|Defined|p39|middle Pleistocene|early Pleistocene|Formerly known as Millstream Calcrete. Early-Mid Pleistocene.||||||07-APR-16
23792|Millstream Dolomite|40987|4|Described|p31|||||||||
23792|Millstream Dolomite|61155|5|Briefly described|p16|Early Miocene|Early Miocene|Overlain by and interfingers with Kangiangi Clay. Age: 23.5-18.5Ma. Thickness: 47m. Geological Province: West Fortescue Valley.||||||
23792|Millstream Dolomite|62021|6|Mentioned|p169|||Alluvium/colluvium.||||||
23792|Millstream Dolomite|65194|5|Briefly described|p15-16, p18, p98, p101-106|Pleistocene|Neogene|max age: Late Neogene. Lower Fortescue valley. The main aquifer. Palaeovalley infill that unconformably overlies the Robe Formation, is unconformably overlain by the Kumina Conglomerate and Kangiangi Clay. Lithology consists of textured dolomite and layers of silcrete, clay and conglomerate. Thickness to 46m.||||||07-APR-16
23792|Millstream Dolomite|73574|5|Briefly described|p762, p770|Pleistocene|Miocene|Main aquifer in the lower Fortescue Valley.|||||Dolomite, calcareous dolomite, calcrete; with silcrete, clay, chert breccia and local basal conglomerate.|
25238|Millyit Formation|29813|6|Mentioned|Table 4|||||||||
25238|Millyit Formation|41730|6|Mentioned|Fig.3|||||||||
25238|Millyit Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
31124|Milyit Sandstone|43173|6|Mentioned|54|Early Triassic|Late Permian|||||||
31124|Milyit Sandstone|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Canning Basin.||||||
39438|Mimosa submember|22754|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Informal unit of the Camp Shale member (Koongie Park Formation).  Max. thickness: <80m.||||||07-NOV-08
31936|Minchin siltstone|43876|14|Not recorded|p581||Early Jurassic|||||||
75174|Mindoola Tonalite|64891|5|Briefly described|p37 Fig. 2|Archean|Archean|May be misspelt? - see also Mindoolah Tonalite (p50 Tb. 1). Geological province: Murchison Domain.||||||07-FEB-11
75174|Mindoola Tonalite|67129|5|Briefly described|p19 Fig.20|Archean|Archean|Murchison Domain, Youanmi Terrane.||Annean Supersuite.|||Syn-volcanic tonalitic rocks.|
75174|Mindoola Tonalite|69583|6|Mentioned|p52|||Murchison Domain.||||||
77096|Minerie Sequence|63980|4|Described|p57.|Archean|Archean|Tholeiitic and komatiitic basalts, with associated ultramafic cumulates. Volcaniclastic sandstone dated.|2698 +/- 5 Ma.|||Overlies Kurnalpi Sequence.||26-SEP-14
77096|Minerie Sequence|64633|5|Briefly described|p4 Fig.3. |||Kurnalpi Terrane.|2705 - 2702 Ma.|||Overlies Kurnalpi Sequence.||
77096|Minerie Sequence|66880|5|Briefly described|p9, p27. |Archean|Archean|Term used in this study for the upper part of the Kurnalpi Sequence. Kurnalpi Terrane. Seamount-type mafic-ultramafic volcanism.|2698 +/- 5 Ma.|Unit in Kurnalpi Sequence.|||Basalt-dolerite-gabbro-komatiite sequence, with minor sedimentary rocks.|
77096|Minerie Sequence|67198|5|Briefly described|p5 Fig.2, p7, p46-49|Neoarchean|Neoarchean|Kurnalpi Terrane.|2698 +/- 5 Ma (Kositcin et al, 2008)|||Conformably overlies the Kurnalpi Sequence|Pillow basalt, dolerite and high Mg basalt (the Murrin Murrin komatiite), with minor sedimentary rocks.|11-SEP-17
77096|Minerie Sequence|70020|5|Briefly described|p121|Neoarchean|Neoarchean|Geological province: Kurnalpi Terrane, Yilgarn Craton.||||Underlain by Kurnalpi Sequence.|Basalt; komatiitie and komatiitic basalt, intermediate volcanic/volcaniclastic rocks.|
77096|Minerie Sequence|70087|6|Mentioned|p215, 222-223, 225|Archean|Archean||2698 +/- 3 Ma (Barley et al., 2008).|||Conformably overlies (or is tectonically interleaved with) the Kurnalpi Sequence. Corresponds to the Kambalda Sequence in the Kalgoorlie Terrane.|Felsic volcaniclastics with numerous mafic units.|
77096|Minerie Sequence|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kurnalpi Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.||||||
77096|Minerie Sequence|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Kurnalpi Sequence.||
77096|Minerie Sequence|71308|6|Mentioned|p711 Fig.2|||Kurnalpi Terrane.||||||
77096|Minerie Sequence|71309|6|Mentioned|p740 Fig.3|||||||||
77096|Minerie Sequence|72485|6|Mentioned|p3 Fig.2|||||||||
73873|Mingah tuff member|24590|6|Mentioned|p30 Fig. 1.3|Archean|Archean|Informal name. Of the Tumbiana Formation (Fortescue Group). Pisolitic and felsic tuff.||||||07-FEB-11
78753|Minger Tuff Member|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean|[Mis-spelling of Mingah]||Unit in Tumbiana Formation.||Is overlain by Meentheena Carbonate Member.||
29780|Minier Formation|43037|6|Mentioned|p26|||Misspelling of Mininer Turbidite Member||||||
34383|Minier Supersequence|22682|5|Briefly described|Fig21,p31|Orosirian|Orosirian|1953-1906 Ma. Ashburton Province||||||03-MAR-10
33210|Minilya Sub-Group|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
33210|Minilya Sub-Group|45015|5|Briefly described|map legend||Artinskian|Of the Byro Group. Includes: Cundlego Formation, Quinanie Shale, Wandagee Formation, Norton Greywacke and Baker Formation. Geological Province: Carnarvon Basin.||||||31-MAY-06
33210|Minilya Sub-Group|61958|5|Briefly described|Map sheets 1 and 2|Artinskian|Artinskian|Includes: Cundlego Formation, Quinnanie Shale, wandagee Formation, Norton Greywacke and Baker Formation.||||||21-MAR-06
33209|Minilya Sub-group|44532|14|Not recorded|p.7, map|||(G50-5).||||||
25241|Minilya Subgroup|23815|5|Briefly described|p286|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Byro Group.||||||27-APR-05
25241|Minilya Subgroup|36890|3|Fully described|p286|||||||||
25241|Minilya Subgroup|37295|6|Mentioned|p54|||||||||
25241|Minilya Subgroup|44344|2|Defined|p.11,,13-15|||upper subgroup of Byro Group. Contains Cundlego Formation, Quinnanie Shale, Wandagee Formation, Norton Greywacke & Baker Formation. (top). (G50-1).||||||
25241|Minilya Subgroup|44345|14|Not recorded|map legend?|||Age unknown?||||||
25241|Minilya Subgroup|45016|2|Defined|p.155-159||Artinskian|Tb, p.125,126,174,180. (F50-13,G50-1,5). "Minilya Group" - Defn on Tech. File G/50-1.||||||
29781|Mininer Formation|43037|6|Mentioned|p32|||Same as Mininer Turbidite Member||||||
70013|Mininer Turbidite|61526|5|Briefly described|p880|||Abbreviated version of Mininer Turbidite Member. Of the Ashburton Formation. Proximal, with coarse components.||||||
75797|Mininer supersequence|24607|5|Briefly described|p968|||Lower, sandstone-rich part of the Ashburton Formaton. Deep marine basin.||||||
26032|Miningarra Subgroup|7471|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||Unit in Earaheedy Group.|Includes Wandiwarra Formation.|Overlies Tooloo Subgroup.||
26032|Miningarra Subgroup|23253|5|Briefly described|p2|||See unnumbered figure. Geological Province:  Earaheedy Basin.||||||12-SEP-05
26032|Miningarra Subgroup|23529|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Max. thickness: >2500m. Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group, Earaheedy Basin||||||07-NOV-08
26032|Miningarra Subgroup|23589|4|Described|p3|||Of Earaheedy Group. Underlain by Tooloo Subgroup.||||||17-JUL-08
26032|Miningarra Subgroup|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|23890|5|Briefly described|p21 Fig.11|||Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||
26032|Miningarra Subgroup|24017|5|Briefly described|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|24021|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Parent: Earaheedy Group.   Geological Province: Earaheedy Basin||||||07-NOV-08
26032|Miningarra Subgroup|24578|4|Described|p776 Fig.1, p778 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Overlies the Tooloo Subgroup, Geological Province: Earaheedy Basin||||||07-NOV-08
26032|Miningarra Subgroup|31217|2|Defined|p41|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
26032|Miningarra Subgroup|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26032|Miningarra Subgroup|40938|4|Described|p15|||||||||
26032|Miningarra Subgroup|43595|5|Briefly described|p346|||||||||
26032|Miningarra Subgroup|50188|5|Briefly described|p2, p3, Fig. 1|||Of the Earaheedy Group. Overlies Tooloo Subgroup. Maximum Thickness: 2500m. Geological Province: Earaheedy Basin.||||||16-JUL-08
26032|Miningarra Subgroup|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Includes the Chiall Formation.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|50222|5|Briefly described|p320 Fig. 3, p329|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Comprises Chiall and Wongawol Formations.  Overlies the Tooloo Subgroup.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Comprises Chiall, Wongawol, Kulele and Mulgarra formations.  Kulele formation in this instance refers to Kulele Limestone, Mulgarra formation refers to Mulgarra Sandstone.  Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|50224|5|Briefly described|p368|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Comprises Chiall and Wonawol Formations, Kulele Limestone and Mulgaraa Sandstone. Geological Province: Earaheedy Basin.||||||07-FEB-11
26032|Miningarra Subgroup|50226|5|Briefly described|p423, p424 Fig. 5|||Of the Earaheedy Group.  Comprises the Chiall and Wongawol Formations, Kulele Limestone and Mulgarra Sandstone.  Overlies the Tooloo Subgroup.  Geological Province: Earaheedy Basin.||||||24-JUN-04
26032|Miningarra Subgroup|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin. Of the Earaheedy Group. Overlies Tooloo Subgroup.||||||26-MAY-09
26032|Miningarra Subgroup|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin||||||07-NOV-08
26032|Miningarra Subgroup|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Overlies Tooloo Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|61564|5|Briefly described|p590 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: <1.85Ga. Geological Province: Earaheedy Basin.||||||07-NOV-08
26032|Miningarra Subgroup|64580|6|Mentioned|map legend|||||||||
26032|Miningarra Subgroup|64725|6|Mentioned|p59.|||||Upper unit in Earaheedy Group.|Consists of Chiall and Wongawol Formations, Kulele Limestone and Mulgarra Sandstone.|Overlies Tooloo Subgroup.||03-APR-12
26032|Miningarra Subgroup|64772|4|Described|p9, p12, p10 Fig. 5, p43|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Comprises Chiall and Wongawol Fms., Kulele Limestone and Mulgarra Sandstone. Overlies the Tooloo Subgroup. Total thickness: at least 2500m. On Plate 1, Miningarra Subgroup not shown, and Chiall Formation shown within Tooloo Subgroup.||||||25-NOV-13
26032|Miningarra Subgroup|65264|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Upper part of the Earaheedy Group. Geological province: Earaheedy Basin.||||||07-FEB-11
26032|Miningarra Subgroup|65419|6|Mentioned|p46.|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.||Unit in Earaheedy Group.||||
26032|Miningarra Subgroup|65472|5|Briefly described|p1, p3 Fig.2, p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. On p3 Fig.2, Miningarra Subgroup range not shown to include Kulele Limestone and Mulgarra Sandstone, but does in p1 description and in Fig 4.||Of Earaheedy Group|Includes Chiall Formation, Wongawol Formation, Kulele Limestone and Mulgarra Sandstone, in ascending order|Overlies Tooloo Subgroup.||24-SEP-15
26032|Miningarra Subgroup|65692|5|Briefly described|p9, p55-56|||||Earaheedy Group.|Chiall, Wongawol, Kulele and Mulgarra Formations.|Overlies Tooloo Subgroup.||
26032|Miningarra Subgroup|66427|5|Briefly described|p39, p41 Tb.1, p43-44, p47-51           |||See also p63, p65, p69-74. Redefined here: Wandiwarra Formation and Princess Ranges Quartzite become Members of Chiall Formation, along with Karri Karri Member. Contains 1.8 Ga detrital zircon in topmost Formation.||Of the Earaheedy Group.|Includes the Chiall Formation, Wongawol Formation, Kulele Limestone and Mulgarra Sandstone.|Overlies the Tooloo Subgroup.|Predominantly siliciclastic, but includes stromatolite-bearing carbonate sequences. Basal conglomerate entirely of underlying Windidda Member cobbles and boulders in an ironstone matrix.|
26032|Miningarra Subgroup|68055|5|Briefly described|p77-78|Proterozoic|Proterozoic|Earaheedy Basin.||Earaheedy Group.|Chiall, Wongawol Formations; Kulele Limestone; Mulgarra Sandstone.|Overlies Tooloo Subgroup.|Predominantly high-energy siliciclastic rocks with some stromatolitic carbonate sequences.|
26032|Miningarra Subgroup|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|||||Earaheedy Group|Includes Chiall Formation, Wongawol Formation, Mulgarra Sandstone.|||
26032|Miningarra Subgroup|71270|5|Briefly described|GEOL_LUT_CSV files|||Geological province: Capricorn Orogen. Of Earaheedy Basin. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.||Unit of Earaheedy Group.|Includes Chiall Formation, Mulgarra Sandstone.|||
26032|Miningarra Subgroup|71484|6|Mentioned|p122|||Superseded and status changed to Group status by Martin et al., 2016; Sheppard et al., 2016. See Miningarra Group.||Unit of Earaheedy Group.||||30-AUG-19
78450|Miningarra Trondhjemite|65827|6|Mentioned|p57|Paleoarchean|Paleoarchean|Informal name (of Sims and Carson 2001) for the Walgunya Trondhjemite.||||||16-OCT-13
78450|Miningarra Trondhjemite|69041|4|Described|p9, p19|||Pilbara Craton. Forms an oval shaped pluton of c. 5km maximum diameter along the northeastern margin of the Mount Edgar Igneous Complex. Outcrop is limited to rare scattered boulders. This unit is moderately foliated and has a moderate radiometric total count and moderate magnetic susceptibility.|||||Medium- to coarse-grained, quartz rich, biotite trondhjemite containing quartz, plagioclase, biotite and accessory magnetite.|
40547|Minjar Group|23955|4|Described|p1240, p1242 Fig.3|||Overlies the Thundelarra Group. Maximum Thickness: >3700m. Geological Province: Murchison province, Yilgarn Craton.||||||
40547|Minjar Group|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Murchison Supergroup.|Gossan Valley, Golden Grove, Scuddles Formations.|||
40547|Minjar Group|69584|6|Mentioned|p5 Fig.2|Mesoarchean|Mesoarchean|||Murchison Supergroup|Gossan Valley Formation, Golden Grove Formation, Scuddles Formation,|||
40547|Minjar Group|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Murchison Supergroup.|Gossan Valley, Golden Grove, Scuddles Formations.|Overlies Weld Range Group. Is overlain unconformably by Norie Group.||
40547|Minjar Group|70020|5|Briefly described|p131|||Geological province: Yilgarn Craton. Thickness: >3700m.||Unit of Murchison Supergroup.||Underlain by Thundelarra Group.||
40547|Minjar Group|70270|5|Briefly described|p519, p519 Fig. 2, p520 Fig. 3|||Probably after Clifford, 1992 PhD. Murchison Province.||Of Murchison Supergroup.||||29-JUN-18
40547|Minjar Group|71168|5|Briefly described|p11, p12 fig 6, p13 fig 7|||Yilgarn Craton.||||Overlies the Thundelarra Group.||
31954|Minnie Creek Supersuite|24197|5|Briefly described|p69-70|||Incl: Aurilla Creek, Minnie Creek, Landor and Mount Marquis Batholiths; Yinnetharra, Conndoondoo and Dalgetty Gneiss domes (Williams 1986). Oxidised and fractionated. Geol.P: Gascoyne Province. See also Minnie Creek Suite - names used interchangeably.||||||07-FEB-11
31954|Minnie Creek Supersuite|50425|5|Briefly described|p1.1, 1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Age: 1800Ma.||||||07-NOV-08
40448|Minnie Creek granite|24602|5|Briefly described|p857|||Late stage granitoid of the Gascoyne complex. Informal name. Age: 1795 +/- 8 Ma. See also p855.||||||
74603|Minningarra Subgroup|64284|5|Briefly described|p58 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group. Comprises Chiall, Wongawol Formations, Kulele Limestone and Mulgarra Sandstone. Overlies Tooloo Subgroup. Geological Province: Earaheedy Basin.||||||07-FEB-11
74603|Minningarra Subgroup|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Upper division of Earaheedy Group; overlies Tooloo Subgroup. Comprises Chiall, Wongawol and Kulele Formations and Mulgarra Sandstone. Total thickness: 2700m. Geological province: Earaheedy Basin. Clastic and carbonate rocks.||||||07-FEB-11
74603|Minningarra Subgroup|64724|6|Mentioned|p45 Fig.5|Statherian|Statherian|Earaheedy Basin. Deposited during the Leichhardt Extension (1800-1750 Ma).||Of Earaheedy Group.||||02-APR-12
74603|Minningarra Subgroup|67855|6|Mentioned|p207, p208 fig 3-8|Paleoproterozoic|Paleoproterozoic|||Earaheedy Group|Includes Wandiwarra Formation, Princess Ranges Quartzite, Wongawol Formation, Kulele Limestone, Mulgarra Sandstone.|||
74603|Minningarra Subgroup|69313|5|Briefly described|p23, p25 Fig.4.3, p57 Fig.6.3|Paleoproterozoic|Paleoproterozoic|2900m thick. Deposited in low energy marine environment. See also  p61, p92, p101.||Earaheedy Group|Chiall Formation, Wongawol Formation, Kulele Limestone, Mulgarra Sandstone.|Unconformably overlies the Frere Formation.|Coarsening-upwards sequence of shale, siltstone, mudstone, sandstone and intraclastic breccias.|08-SEP-17
41369|Minno augen gneiss|44109|5|Briefly described|p136|Mesoproterozoic|Mesoproterozoic|Syn-metamorphic foliated granite located south of the Kalka intrusion near Mount Davies. Age: 1198+/-6Ma (SHRIMP U-Pb). See also p140 Fig. 150.||||||
41369|Minno augen gneiss|50607|5|Briefly described|p2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Of the Kulgera Supersuite. Age: 1198 +/- 6Ma (U-Pb).||||||
31148|Minum Cove Member|43495|6|Mentioned|20|||Of Tamala Limestone? Near Perth.||||||14-JAN-13
41437|Minyari Gneiss|50436|6|Mentioned|p4.2|||Superseded by Koolyu Granite.||||||
41438|Minyari Group|50436|5|Briefly described|p4.1|Neoproterozoic|Neoproterozoic|Includes: O'Callaghans Granite, Minyari Granite, Koolyu Granite. Of the O'Callaghans Supersuite. Geological Province: Paterson Orogen.||||||
77212|Minyari monzogranite|64943|5|Briefly described|p25 Table 4|Neoproterozoic|Neoproterozoic|633+/-13 Ma by SHRIMP U-Pb (Nelson 1995).||||||
77089|Mira Marl|6876|6|Mentioned|p100 Fig.5.|Paleogene|Paleogene|||||||
34996|Miralga Creek Porphory|23046|6|Mentioned|169|||||||||
77231|Mirturtu suite|66256|5|Briefly described|p8, p18 Fig.14, p23-31, see comments|Stenian|Stenian|Age: late Musgravian. Walpa Pulka Zone. Compositionally heterogeneous throughout. Geochemistry provided. Age: SHRIMP Whole rock Nd isotopic crystallization age. See also p34-36, p38, p41, p43-44, p54 App.1, p63-64 App.3, p71 App.4.|1181+/-6 Ma to 1175+/-15 (GSWA)|Pitjantjatjara Supersuite|||Granite.|11-JAN-17
77231|Mirturtu suite|67375|6|Mentioned|p25 Fig.17, p26 Fig.19. |Mesoproterozoic|Mesoproterozoic|A-type. Within-plate, Yb-enriched granite. Late Musgrave Orogeny.||Unit in Pitjantjatjara Supersuite.||||
77231|Mirturtu suite|67553|6|Mentioned|p27-28,33,67|||Geological province: Musgrave Province, North Australian Craton. Late Musgravian granite.||Unit of Pitjantjatjara Supersuite.||||
77231|Mirturtu suite|69091|5|Briefly described|p64 Fig.4.10|||late Musgravian granite||Pitjantjatjara Supersuite|||Granite.|
77231|Mirturtu suite|69729|5|Briefly described|p74 Fig.7, p77-78|||Geochemistry plots.||Pitjantjatjara Supersuite.|||A-type granites.|
31154|Mission Basalt|43496|6|Mentioned|6|||||||||
78641|Mission Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 3 unnamed subunits.||Peridotite; pyroxenite; gabbro; all metamorphosed.|06-AUG-15
78641|Mission Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Peridotite, pyroxenite and gabbro; metamorphosed.|
78641|Mission Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro, peridotite and pyroxenite; metamorphosed.|
41087|Missouri basalt|24139|5|Briefly described|p239 Table 1|||Geological Province: Ora Banda Domain.  Of the Pole Group.||||||
78869|Miturtu Monzogranite|69153|5|Briefly described|GEOCHRON files|||See GEOCHRON/180300.1.pdf, 180299.1.pdf and 180256.1.pdf (publ. 2006).|1181+/-6 Ma; 1203+/-16 Ma, 1175+/-15 Ma||||Porphyritic metamonzogranite forms inclusions within porphyritic grey granite|02-SEP-14
73561|Modern Veneer|36483|3|Fully described|p74|||Informal name applied to sediments forming a thin veneer over older units (Semeniuk 1980) - used in general for the recent sediments, which may be seasonal, over Mowanjum Sand, Airport Creek  and  Double Nob Formations and Christine Point Clay.||||||
25249|Molecap Greenstone Member|41989|5|Briefly described|p115|||||||||
25250|Mollyella Adamellite|38335|6|Mentioned|p1727|||Misspelling of Moolyella||||||
28208|Mondana Adamellite|31308|6|Mentioned|p70|||||||||
28208|Mondana Adamellite|31853|6|Mentioned|p61|||||||||
28208|Mondana Adamellite|37633|6|Mentioned|p129|||||||||
28208|Mondana Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2.||||||07-NOV-08
28208|Mondana Adamellite|39672|6|Mentioned|p238|||||||||
28208|Mondana Adamellite|39697|3|Fully described|p44|||||||||
28208|Mondana Adamellite|41636|5|Briefly described|p63|||||||||
28208|Mondana Adamellite|44150|5|Briefly described|p146 Tb.2-21, p150 Fig.2-138|||280 sq. km. Post-tectonic granitoid.||Corunna Downs Granitoid Complex||Intrudes Warrawoona Group and Carbana Pool Adamellite.|Biotite monzogranite, biotite-hornblende monzogranite.|
28208|Mondana Adamellite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Replaced by Mondana Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
28208|Mondana Adamellite|64327|6|Mentioned|p64|Archean|Archean|Superseded by Mondana Monzogranite. Written as "Mondana Adamellite".||||||07-NOV-08
28208|Mondana Adamellite|65827|6|Mentioned|p29|Mesoarchean|Mesoarchean|Former name of Mondana Monzogranite.
||||||
81215|Mondana Suite|69041|4|Described|p10-p11, p19|Paleoarchean|Paleoarchean|Pilbara Craton. Of the Corunna Downs Igneous Complex (used in the province sense). Forms an elliptical shaped body in the southeast and east of the Complex. Outcrop ranges from rubble, boulder, to small tors and slabs. The suite has well defined intrusive contacts. contains three unnamed units. This suite is locally foliated and contains enclaves of Boobina Porphyry. Monzogranites have moderate total counts and low magnetic susceptibility.|3317 +/- 2 Ma (Barley & Pickard, 1999 SHRIMP)||||Fine- to coarse-grained, quartz-rich, biotite monzogranite with seriate to sparsely developed feldspar porphyritic texture.|21-JUN-19
25252|Mondana granite|37373|6|Mentioned|Table 2.VI|||||||||
28763|Monksleigh Sandstone""|31910|6|Mentioned|p22|||Refers Johson et al. (1954)||||||
28763|Monksleigh Sandstone""|33166|6|Mentioned|p63|||Refers Fairbridge (1953)||||||
25254|Mons Cupri Adamellite|39580|4|Described|p294|||||||||
25254|Mons Cupri Adamellite|44150|6|Mentioned|p141 Tb.2-20|||Geochemical analysis presented.||||||
38840|Mons Cupri Dacite|24140|5|Briefly described|p214 Fig. 1, p217 Fig. 2|||Of the Whim Creek Group. Dacitic intrusions. Geological Province: Mallina Basin||||||
38840|Mons Cupri Dacite|24191|3|Fully described|p829, p831|Archean|Archean|See also p830 Fig. 2.  Of Whim Creek Group. Along with Red Hill Volcanics, supersedes Mons Cupri Volcanics.  Intrudes Red Hill Volcanics.  Geological Province: Pilbara Craton.||||||07-NOV-08
38840|Mons Cupri Dacite|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Dacitic intrusions. Intrudes the Red Hill Volcanics.  Age: ca 3010Ma. Thickness: 200m. Geological Province: Pilbara Craton.||||||07-FEB-11
38841|Mons Cupri Dacite member|24191|5|Briefly described|p829, p831|Archean|Archean|Informal - see Mons Cupri Dacite.  Name used interchangeably with Mons Cupri Dacite.  Thickness at Red Hill: 160m.  Geological Province: Pilbara Craton.||||||07-NOV-08
26038|Mons Cupri Volcanics|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3000-2900Ma.||||||07-NOV-08
26038|Mons Cupri Volcanics|23244|5|Briefly described|p19,24 Fig.5||Archean|Age: SHRIMP U-Pb Zircon age of 2991+/-12Ma. of Whim Creek Group.||||||07-NOV-08
26038|Mons Cupri Volcanics|23255|6|Mentioned|Fig.2|||||||||
26038|Mons Cupri Volcanics|23348|5|Briefly described|220|||||||||
26038|Mons Cupri Volcanics|23743|4|Described|p4|Archean|Archean|Of Whim Creek Group. Overlain by Cistern Formation. Underlain by Cleaverville Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
26038|Mons Cupri Volcanics|23784|4|Described|p22|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
26038|Mons Cupri Volcanics|23789|5|Briefly described|p24|||Now divided into Mons Cupri dacite and Red Hill volcanics.  Geological Province: Pilbara Craton.||||||
26038|Mons Cupri Volcanics|23793|4|Described|p21|Archean|Archean|Of Whim Creek Group||||||07-NOV-08
26038|Mons Cupri Volcanics|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whim Creek Group. Overlain by Cistern Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
26038|Mons Cupri Volcanics|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Whim Creek Group.  Age: c.3.01Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
26038|Mons Cupri Volcanics|23936|4|Described|Tb.1|Archean|Archean|Age: c.3.01-2.99 Ga. Geological Province: Pilbara Craton. Overlain by Cistern Formation. Underlain by Warrambie Basalt.||||||07-NOV-08
26038|Mons Cupri Volcanics|24023|4|Described|p19|Archean|Archean|Of Whim Creek Group. Maximum thickness: 1000m.||||||07-NOV-08
26038|Mons Cupri Volcanics|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Whim Creek Group. Geological Province: Pilbara Craton||||||07-NOV-08
26038|Mons Cupri Volcanics|24140|5|Briefly described|p216|Archean|Archean|Of Fitton (1975) and Smithies (1997). Both included it in Whim Creek Group. Replaced by Mons Cupri Dacite in this study.||||||07-NOV-08
26038|Mons Cupri Volcanics|24184|5|Briefly described|p715 Fig.11|Archean|Archean|Of the Whim Creek Group. Overlain by Cistern Formation. Underlain by Warambie Basalt. Geological Province: Mallina Basin. Age:<3010Ma||||||07-NOV-08
26038|Mons Cupri Volcanics|24191|5|Briefly described|p829, p831|Archean|Archean|Superseded by Mons Cupri Dacite and Red Hill Volcanics.  Geological Province: Pilbara Craton.||||||07-NOV-08
26038|Mons Cupri Volcanics|24192|5|Briefly described|p860|Archean|Archean|Of the Whim Creek Group. Geological Province: Pilbara Craton||||||07-NOV-08
26038|Mons Cupri Volcanics|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
26038|Mons Cupri Volcanics|31310|6|Mentioned|p53|||||||||
26038|Mons Cupri Volcanics|34829|6|Mentioned|p67|||||||||
26038|Mons Cupri Volcanics|36551|6|Mentioned|p59|||||||||
26038|Mons Cupri Volcanics|37373|4|Described|p80|||||||||
26038|Mons Cupri Volcanics|38498|5|Briefly described|Table 1|||||||||
26038|Mons Cupri Volcanics|38544|6|Mentioned|Fig.1|||||||||
26038|Mons Cupri Volcanics|39697|3|Fully described|p108|||||||||
26038|Mons Cupri Volcanics|39837|6|Mentioned|Table 1|||||||||
26038|Mons Cupri Volcanics|41073|4|Described|p206|||||||||
26038|Mons Cupri Volcanics|41250|4|Described|p30|||||||||
26038|Mons Cupri Volcanics|41252|6|Mentioned|Table 1|||||||||
26038|Mons Cupri Volcanics|41263|6|Mentioned|p57|||||||||
26038|Mons Cupri Volcanics|42231|6|Mentioned|p334|||||||||
26038|Mons Cupri Volcanics|42973|5|Briefly described|p175|||||||||
26038|Mons Cupri Volcanics|43595|5|Briefly described|p213|||||||||
26038|Mons Cupri Volcanics|43698|6|Mentioned|p26|||||||||
26038|Mons Cupri Volcanics|43769|5|Briefly described|p860|||Also 'Mons Cupri Formation'.||||||27-AUG-07
26038|Mons Cupri Volcanics|43821|5|Briefly described|map legend|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
26038|Mons Cupri Volcanics|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-132, p137|||||Whim Creek Group|||Felsic volcanics with tuffaceous and volcaniclastic material at top and bottom; dacitic to rhyolitic lava, tuff and agglomerate in the middle. Intruded by feldspar-phyric dacite plugs.|
26038|Mons Cupri Volcanics|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
26038|Mons Cupri Volcanics|63441|5|Briefly described|p5 Tb.1, p6 Tb. 1|Archean|Archean|Redefined as Mons Cupri Dacite Member of the Red Hill Volcanics, in the Whim Creek Basin (Pilbara Craton).||||||07-FEB-11
26038|Mons Cupri Volcanics|65415|4|Described|p119 Fig.1, p120, p121.|Archean|Archean|Previously included a boulder conglomerate marker horizon, which is now included in the Cistern Formation (Smithies, in prep.).||Basal unit in Whim Creek Group.|Includes Warambie Basalt and Mount Brown Rhyolite Member.|Locally interfingers with Warambie Basalt. Is intruded by Opaline Well Complex. Is overlain by Mallina Formation.|A homogeneous sequence dominated by felsic lavas and massive pyroclastics; volcaniclastic and clastic rocks are rare.|
26038|Mons Cupri Volcanics|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv|c. 3009 Ma||Geological province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. Superseded; see Red Hill Volcanics.||||||
26038|Mons Cupri Volcanics|70775|5|Briefly described|p51-p52|||Informal name from Fitton et al (1965) and Hickman (1977). This unit was made obsolete by Pike et al., 2002 and renamed the Red Hill Volcanics.||||||
38692|Mons Cupri dacite|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of Whim Creek Group.  Formerly grouped with Red Hill volcanics as Mons Cupri Volcanics.  Max. thickness: 160m.  Geological Province: Pilbara Craton.||||||07-NOV-08
38692|Mons Cupri dacite|24140|5|Briefly described|p216, p217|Archean|Archean|Previously known as Mons Cupri Volcanics (Fitton et al 1975; Smithies 1997). Of the Whim Creek Group. Age: 2991+/-12Ma (Barley et al 1994). Max. thickness: 160m. Geological Province: Mallina Basin||||||07-NOV-08
38692|Mons Cupri dacite|70775|5|Briefly described|p52|||This informal name was used by Pike et al ., 2002 instead of the Mount Brown Rhyolite and Mount Brown Rhyolite Member as they regarded this unit as separate formation to the Red Hill Volcanics.|||||Well-bedded sandstone and siltstone, massive volcaniclastic sandstone, polymictic conglomerate and breccia.|
81307|Montague granodiorite|70020|6|Mentioned|p130|Neoarchean|Neoarchean|Spatially and temporally associated with VHMS mineralization in the Gum Creek greenstone belt.|2722+\-7 Ma|||||
81307|Montague granodiorite|73596|6|Mentioned|p1167|Neoarchean|Neoarchean|Southern Cross Domain.|2722 +/- 7 Ma (Wang et al., 1998).|||||
80418|Montague monzogranite|70020|6|Mentioned|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||||||
80418|Montague monzogranite|71168|6|Mentioned|p7, p50 Fig. 29|Neoarchean|Neoarchean|Gum Creek greenstone belt, Murchison Domain [or Southern Cross Domain?], Youanmi Terrane, Yilgarn Craton.||||||07-FEB-18
75191|Montara beds""|5952|5|Briefly described|p216|||Of Young et al. (1995). Broadly equivalent to the Elang Formation.||||||01-MAR-10
30742|Monument Formation (WA)|23815|6|Mentioned|p281|||Geological Province: Carnarvon Basin. Equivalent to the One Gum and Keogh Formations.||||||
30742|Monument Formation (WA)|36890|6|Mentioned|p281|||||||||
30742|Monument Formation (WA)|37295|6|Mentioned|Table 2|||||||||
30742|Monument Formation (WA)|44217|14|Not recorded|Fig.3|||||||||
30742|Monument Formation (WA)|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group.||||||01-JUN-06
30742|Monument Formation (WA)|45016|2|Defined|p103-108||Artinskian|Tb, Fig.65, p.73,74,77,97,111,115,116,119,144,148. (G50-6,9,10).||||||
30742|Monument Formation (WA)|48885|14|Not recorded|p.9,10,13,Pl.2|||(G/50-6).||||||
30742|Monument Formation (WA)|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
39350|Monument Monzogranite|24091|4|Described|p88|Archean|Archean|Age: 2659+/-2Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
39350|Monument Monzogranite|24196|5|Briefly described|p46|Archean|Archean|Age: 2659 +/- 2 Ma (Fletcher et al., 2001).||||||07-NOV-08
81379|Monument Ultramafic|70326|5|Briefly described|p360,364|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton.||||Correlable to Redeemer and Bent Tree basalts?|Spinifex-textured komatiite.|
75826|Monument Ultramafic Unit|66192|5|Briefly described|p544, p545 Fig.2|||In Agnew-Wiluna Greenstone Belt. Thin spinifex flows. Considered unprospective.||||||09-MAR-12
75826|Monument Ultramafic Unit|70275|6|Mentioned|p471, 480|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||Overlies Centenary Bore Basalt. Is overlain by Vivien Sedimentary Formation.||
75826|Monument Ultramafic Unit|70276|6|Mentioned|p783-784, 787|||Presented as [very informal] Monument ultramafic unit. Mount Keith area, Agnew-Wiluna greenstone belt, Yilgarn Craton. Comprises thin (<1m-thick) flow units; distal extrusive facies. Unmineralised and unprospective.|||||Comprises a series of spinifex-bearing thin flows (<5 - 10m thick).|
38671|Monument monzogranite|23786|5|Briefly described|p52|||Geological Province: Yilgarn Craton.||||||
38671|Monument monzogranite|24196|6|Mentioned|p2, p44|||Geological Province: Yilgarn Craton.||||||28-MAY-04
81348|Moodini granite|70084|5|Briefly described|p219-220,229|Stenian|Stenian|Geological province: Madura Province. Coeval with Bentley Supergroup deposition, and emplacement of Kullal Dykes and Giles intrusions in the Musgrave Province. Also coeval with, and compositionally similar to Pitjantjatjara Supersuite A-type granites. Shown as Moodinin granites p229.||||||08-AUG-19
40312|Moogaloo Formation|24390|5|Briefly described|p20 Table 5|Early Permian|Early Permian|Geological Province: Southern Carnarvon Basin.||||||
40312|Moogaloo Formation|50085|5|Briefly described|p20 Tb. 5|Early Permian|Early Permian|Geological Province: Southern Carnarvon Basin.||||||
42394|Moogooloo Division""|23815|6|Mentioned|p281|||Superseded by the Moogooloo Sandstone (Condon, 1958). Geological Province: Merlinleigh Sub-basin.||||||14-DEC-04
27491|Moola Boola Formation|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27491|Moola Boola Formation|69003|6|Mentioned|p5|||Halls Creek Orogen. See also references to Moola Bulla Formation (p19-20).||||||
27491|Moola Boola Formation|69597|6|Mentioned|p5 fig 2b|||||||||
27491|Moola Boola Formation|70731|6|Mentioned|p268,272-273|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Median density: 2490 kg/m3.||||||
72830|Mooloogool Formation|49896|5|Briefly described|p4 Fig. 1|||Of the Yerrida Group. Includes the Doolgunna and Thaduna Formations with intercalated Killara Formation, and Maraloou Formation intercalated with Killara Formation. ||||||
29920|Mooloogool Subgroup|7471|5|Briefly described|p4, Map legend|Proterozoic|Proterozoic|A rift-basin succession.||Unit in Yerrida Group.|Includes Thaduna, Killara and Maraloou Formations.|Overlies Windplain Subgroup.|Aphyric mafic lavas and intrusive rocks, black shale, siltstone, and carbonate rocks.|
29920|Mooloogool Subgroup|12099|5|Briefly described|p677-8, p677-8 Figs.2 & 4, p683|Paleoproterozoic|Paleoproterozoic|New or redefined unit by Occhipinti et al. (1997). High energy depositional environment.||Unit in Yerrida Group.|Includes Thaduna, Doolgunna, Killara and Maraloou Formations.|Conformably overlies Windplain Subgroup.||04-MAR-13
29920|Mooloogool Subgroup|22501|5|Briefly described|p117|||part of the Yerrida Group||||||
29920|Mooloogool Subgroup|22694|5|Briefly described|p6|||Yerrida Group||||||
29920|Mooloogool Subgroup|22716|5|Briefly described|p229|Paleoproterozoic|Paleoproterozoic|Deposited in the Mooloogool rift.||||||07-NOV-08
29920|Mooloogool Subgroup|22940|4|Described|Fig.1 p3|||Rift succession. See also Table 2 p12. of Yerrida Group.||||||
29920|Mooloogool Subgroup|23151|5|Briefly described|p68 Fig.2|||||||||
29920|Mooloogool Subgroup|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group,Yerrida Basin||||||07-NOV-08
29920|Mooloogool Subgroup|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Yerrida Group in the Yerrida Basin||||||07-NOV-08
29920|Mooloogool Subgroup|23589|4|Described|p18|||Of Yerrida Group.||||||
29920|Mooloogool Subgroup|23593|4|Described|p10|||Of Yerrida Group. Underlying unit Windplain Subgroup. Geological Province:Yerrida Basin.||||||
29920|Mooloogool Subgroup|23597|4|Described|p10|||Of Yerrida Group. Underlying unit Windplain Group.||||||
29920|Mooloogool Subgroup|23600|4|Described|p8|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|23744|5|Briefly described|p2 Fig 1|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|See also page 9. Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|23749|4|Described|p8|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|23759|5|Briefly described|p15|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|23865|5|Briefly described|p169|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|23890|5|Briefly described|p21 Fig.11|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|24021|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin||||||07-NOV-08
29920|Mooloogool Subgroup|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group.  Geological Province: Yerrida Basin.||||||07-NOV-08
29920|Mooloogool Subgroup|43836|5|Briefly described|Map Legend||Proterozoic|||||||
29920|Mooloogool Subgroup|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Yerrida Group.||||||18-MAY-04
29920|Mooloogool Subgroup|44204|5|Briefly described|Map Legend||Proterozoic|||||||
29920|Mooloogool Subgroup|44830|5|Briefly described|Map Legend||Proterozoic|||||||
29920|Mooloogool Subgroup|49893|4|Described|p13|Proterozoic|Proterozoic|Of the Yerrida Group. Geological Province: Yerrida Basin. See also p2 Fig.1.||||||
29920|Mooloogool Subgroup|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Yerrida Group.  Geological Province: Yerrida Basin.||||||
29920|Mooloogool Subgroup|61269|5|Briefly described|p86 Fig.1|Paleoproterozoic|Paleoproterozoic|Of the Yerrida Group.||||||07-NOV-08
29920|Mooloogool Subgroup|61271|5|Briefly described|p104, p105|||Of the Yerrida Group. Arenaceous, argillacous and mafic volcanic rocks.||||||
29920|Mooloogool Subgroup|62289|4|Described|plate 1, p3 Fig. 1, p6-8, p12|Palaeoproterozoic|Palaeoproterozoic|Of Yerrida Group; conformable on Windplain Subgroup; rift basin setting; deposited in a high-energy environment, probably a widening rift structure; contains Thaduna, Doolgunna, Killara, and Maraloou Formations.||||||
29920|Mooloogool Subgroup|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Yerrida Group.|Includes Maraloou Formation, Killara Formation (includes Bartle Member), Thaduna Formation, and Doolgunna Formation.|||14-APR-11
29920|Mooloogool Subgroup|63866|5|Briefly described|p165|||Yerrida Basin.||Yerrida Group|Includes the Doolgunna Formation, Thaduna Formation, Killara Formation and the Maraloou Formation.|Conformably overlies the Windplain Subgroup.||
29920|Mooloogool Subgroup|64161|6|Mentioned|p592|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. U-Pb SHRIMP monazite date c.1843 Ma.||||||21-MAR-12
29920|Mooloogool Subgroup|64724|5|Briefly described|p45 Fig.5, p46|Orosirian|Orosirian|Submarine mass-flow deposits and continental flood basalts of the Yerrida Basin. Deposited at the same time as the Capricorn Orogeny (1830-1780 Ma)||Of Yerrida Group.||||02-APR-12
29920|Mooloogool Subgroup|65264|5|Briefly described|p27, p44 Appdx. 1|||Of the Yerrida Group. Unconformably overlies the Windplain Subgroup. Geological province: Yerrida Basin.||||||07-FEB-11
29920|Mooloogool Subgroup|65408|4|Described|pp82-83, p84 Fig.1, p85|Paleoproterozoic|Paleoproterozoic|Redefined to exclude the Johnson Cairn Formation. Represents a significant change from sag-basin to rift-basin setting.||Upper unit in Yerrida Group.|Includes Thaduna, Doolgunna, Killara and Maraloou Formations.|Locally transitionally overlies Windplain Subgroup|Turbidites and volcanics.|11-APR-12
29920|Mooloogool Subgroup|65411|6|Mentioned|p89 Fig.1.|||||Upper unit in Yerrida Group.|Includes Killara, Maraloou, Doolgunna and Thaduna Formations.|||
29920|Mooloogool Subgroup|65412|5|Briefly described|p97 Fig.1.|Paleoproterozoic|Paleoproterozoic|Interpreted to represent a later rift basin.||Unit in Yerrida Group.||||
29920|Mooloogool Subgroup|65419|2|Defined|p4 Fig.1, p7, p10 Fig.3, p18, pp19-29.|Paleoproterozoic|Paleoproterozoic|Named after Mooloogool Homestead. Several kilometres thick. Age constrained by underlying Windplain Subgroup and overlying Earaheedy Group. Includes the Thaduna, Doolgunna and Maraloou Formations of the former Glengarry Group of Gee and Grey (1993) and the Killara Formation, plus the newly defined Killara Formation, parts of which were previously assigned to the Narracoota Volcanics (Gee and Grey, 1993).|Between 2.2 Ga and 1785 Ma.|Upper unit in Yerrida Group.|Includes Maraloou, Killara, Doolgunna and Thaduna Formations.|Conformably overlies Windplain Subgroup.|Terrigenous clastic, volcaniclastic, mafic extrusive and intrusive rocks.|
29920|Mooloogool Subgroup|65913|5|Briefly described|p2 Fig.1, p5.|Paleoproterozoic|Paleoproterozoic|Rift succession of turbidites deposited concurrently with tholeiitic volcanic rocks.||Unit in Yerrida Group.|Includes Maraloou, Killara, Doolgunna and Thaduna Formations.|||24-MAY-16
29920|Mooloogool Subgroup|68561|5|Briefly described|GLENGARY_GEOLOGYP_LUT.csv||Proterozoic|Yerrida Basin. [replaced by Mooloogool Group]||Yerrida Group||||
29920|Mooloogool Subgroup|70796|5|Briefly described|glengarry_100k_geologyp_lut.csv|||Yerrida Basin. Misspelt? See also Mooloogool Group. Also appears in Glengarry100_2645_stratig.pdf.||Yerrida Group||Includes the Maraloou Formation, Killara Formation, Doolgunna Formation.||
29920|Mooloogool Subgroup|70804|5|Briefly described|p2, p37, p45|||Forms the eastern part of the former 'Glengarry Basin'. Developed in a rift basin.||Yerrida Group|Includes the Maraloou Formation, Killarra Formation, Doolgunna Formation, Thaduna Formation.|||
29920|Mooloogool Subgroup|71484|6|Mentioned|p122,124|||Abandoned, see Mooloogool Group (Pirajno et al., 2004).||Unit of Yerrida Group.||||30-AUG-19
27200|Moolyella Adamellite|24590|6|Mentioned|p51 Fig. 2.10|Archean|Archean|See also Moolyella Adamellite Suite and Mooluyella Suite. Names are used interchangeably. Age: <3240Ma. See also p86 and p188.||||||07-FEB-11
27200|Moolyella Adamellite|30485|6|Mentioned|p74|||Refers Hickman & Lipple (1974)||||||
27200|Moolyella Adamellite|31308|6|Mentioned|Table 12|||Geochronology||||||
27200|Moolyella Adamellite|35641|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27200|Moolyella Adamellite|37460|6|Mentioned|p126|||||||||
27200|Moolyella Adamellite|37633|5|Briefly described|Plate 2|||See also P17 and Plate 1.||||||
27200|Moolyella Adamellite|38498|6|Mentioned|p63|||||||||
27200|Moolyella Adamellite|38510|6|Mentioned|Table 1|||||||||
27200|Moolyella Adamellite|38541|6|Mentioned|p381|||||||||
27200|Moolyella Adamellite|38763|6|Mentioned|p104|||||||||
27200|Moolyella Adamellite|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27200|Moolyella Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also P7 & Table 2||||||07-NOV-08
27200|Moolyella Adamellite|39697|3|Fully described|p42|||||||||
27200|Moolyella Adamellite|40596|6|Mentioned|p66|||||||||
27200|Moolyella Adamellite|40933|4|Described|p39|||||||||
27200|Moolyella Adamellite|41624|6|Mentioned|Fig.1|||||||||
27200|Moolyella Adamellite|41938|6|Mentioned|p10|||||||||
27200|Moolyella Adamellite|42785|5|Briefly described|p273|||||||||
27200|Moolyella Adamellite|44150|5|Briefly described|p145 Tb.2-21, p150 Fig.2-138|||See also p155 Fig.2-142. 55 sq. km. Post-tectonic granitoid.|2614 +/- 95 Ma (de Laeter and Blockley, 1972).|Mount Edgar Granitoid Complex|||Albite monzogranite; minor aplite, greisen and pegmatite.|
27200|Moolyella Adamellite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Superseded by Moolyella Monzogranite (Split Rock Supersuite).||||||07-FEB-11
27200|Moolyella Adamellite|69167|6|Mentioned|GA_geochron.csv|Archaean|Archaean|Alternative name for Moolyella Monzogranite. Sample description: Homogenous and even textured felsic biotite-muscovite granite.||||||
27200|Moolyella Adamellite|69590|5|Briefly described|142977.1.pdf|||Nomenclature of Hickman 1983. See Moolyellla Monzogranite.||||||
38962|Moolyella Adamellite Suite|23807|5|Briefly described|p112|Archean|Archean|See also Moolyella Suite.  Geological Province: Pilbara Craton.||||||07-NOV-08
38962|Moolyella Adamellite Suite|24590|5|Briefly described|p41|Archean|Archean|In the centre of the gneiss complex of the Mount Edgar Granitoid Complex. Also referred to as Moolyella Suite. Age: <3240+/11Ma.||||||07-FEB-11
38975|Moonlight Valley tillite|23806|6|Mentioned|p1131|||Informal  - see Moonlight Valley Tillite.||||||07-NOV-06
38975|Moonlight Valley tillite|28255|6|Mentioned|p76|||Informal - see Moonlight Valley Tillite.||||||
31940|Moonyoonooko sandstone|43876|14|Not recorded|p581||Early Jurassic|||||||
22378|Moorehead Formation|64630|5|Briefly described|p31 Fig.2|Sakmarian|Asseliean|Province: Collie Subbasin. Underlies the Westralia Sandstone, overlies the Shotts Formation. Palynology age: to P. confluens. Correlates with the Mosswood Formation. Parent: Stockton Group.||||||24-NOV-09
22378|Moorehead Formation|70774|5|Briefly described|p5 fig 3|Sakmarian|Asselian|Collie Basin.||Stockton Group||Overlies the Shotts Formation. Overlain by the Westralia Sandstone.||
70186|Morapoi Suite|61564|6|Mentioned|p590|||Alkaline rocks of the Yilgarn Craton?||||||
70187|Morapoi Supersuite granitoids|61564|6|Mentioned|p593|||Informal name - both Morapoi Suite and Supersuite are mentioned in this article - same unit or hierarchical?||||||
70188|Morapoi syenite|61564|6|Mentioned|p590|||Informal name. ||||||
26752|Morawa Lava|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26752|Morawa Lava|40347|6|Mentioned|p18|||||||||
26752|Morawa Lava|41957|6|Mentioned|p68|||||||||
28775|Mordor Alkaline Complex|40813|6|Mentioned|p338|||||||||
28775|Mordor Alkaline Complex|69932|6|Mentioned|p308-309, 311|||Located c.50km NE of Alice Springs. Appears in a depleted mantle/Archean crust age diagram. Parent magma may have been derived from lithospheric mantle modified by sediment subduction.|~1130 Ma.||||An alkaline mafic-ultramafic complex.|
70170|Morgan Range gabbro intrusion|44109|5|Briefly described|p94|Mesoproterozoic|Mesoproterozoic|Consists mainly of intensely recrystallised gabbro and mafic granulite intruded by pegmatite and granite veins and cut by northwest and northeast-trending mafic dykes. Within the Blackstone-Jameson region.||||||
70227|Morowa Lavas|24410|6|Mentioned|p142 Tb. 60|||Of the Billeranga Subgroup. ||||||
40202|Morresey Metamorphics|24203|5|Briefly described|p292 Fig. 7|Paleoproterozoic|Paleoproterozoic|Age: <1845Ma.||||||07-NOV-08
33924|Morrisey Metamorphic Suite|22512|6|Mentioned|P284, Fig1 P284|||||||||
33924|Morrisey Metamorphic Suite|23403|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Complex.||||||07-NOV-08
33924|Morrisey Metamorphic Suite|23485|5|Briefly described|p16|||||||||
33924|Morrisey Metamorphic Suite|24410|5|Briefly described|p137 Fig. 80|Paleoproterozoic|Paleoproterozoic|Of the Gascoyne Complex. Quartzite, schist, paragneiss and migmatite.||||||07-NOV-08
33924|Morrisey Metamorphic Suite|49896|5|Briefly described|p16|||Age" 2.0Ga. ||||||
33924|Morrisey Metamorphic Suite|50226|5|Briefly described|p417, p418|||Metasedimentary rocks of the Gascoyne Complex.||||||
69908|Morrisey Metamorphic Suite""|63246|6|Mentioned|p479|||Misspelt - see Morrissey Metamorphics. Medium-grade metasedimentary rocks of the Gascoyne Complex.||||||28-MAY-07
37996|Morrisey Metamorphics|23485|6|Mentioned|p16|||See Morrisey Metamorphic Suite.||||||
27277|Morrissey Metamorphic Suite|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27277|Morrissey Metamorphic Suite|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27277|Morrissey Metamorphic Suite|23312|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes 9 unnamed units that may be metamorphosed equivalents of the Wyloo Group.||||||
27277|Morrissey Metamorphic Suite|23325|5|Briefly described|map legend|Precambrian|Precambrian|In part probable metamorphosed Ashburton Formation, Wyloo Group.||||||
27277|Morrissey Metamorphic Suite|23620|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Complex||||||07-NOV-08
27277|Morrissey Metamorphic Suite|23781|5|Briefly described|p61|||||||||
27277|Morrissey Metamorphic Suite|23976|6|Mentioned|Map Legend|||||||||
27277|Morrissey Metamorphic Suite|23977|6|Mentioned|Map Legend|||||||||
27277|Morrissey Metamorphic Suite|23978|6|Mentioned|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27277|Morrissey Metamorphic Suite|24544|4|Described|p38|Paleoproterozoic|Paleoproterozoic|Previously included Moogie and Camel Hill Metamorphics. Metamorphosed and deformed sediments. Geological Province: Gascoyne Complex.||||||07-NOV-08
27277|Morrissey Metamorphic Suite|37299|6|Mentioned|Fig.1|||||||||
27277|Morrissey Metamorphic Suite|38493|4|Described|p20|||||||||
27277|Morrissey Metamorphic Suite|38817|6|Mentioned|p168|||||||||
27277|Morrissey Metamorphic Suite|39370|2|Defined|p15|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27277|Morrissey Metamorphic Suite|40303|4|Described|p28|||||||||
27277|Morrissey Metamorphic Suite|40937|3|Fully described|p29|||||||||
27277|Morrissey Metamorphic Suite|41971|6|Mentioned|p342|||||||||
27277|Morrissey Metamorphic Suite|41991|6|Mentioned|Fig.2A P128|||||||||
27277|Morrissey Metamorphic Suite|42260|6|Mentioned|p8|||||||||
27277|Morrissey Metamorphic Suite|43255|5|Briefly described|map legend||Proterozoic|||||||
27277|Morrissey Metamorphic Suite|43256|4|Described|5,10||Proterozoic|||||||24-NOV-09
27277|Morrissey Metamorphic Suite|43595|5|Briefly described|p75,342||Paleoproterozoic|||||||07-NOV-08
27277|Morrissey Metamorphic Suite|44142|6|Mentioned|p327 Tb.4-5|||||Gascoyne Complex.||||
27277|Morrissey Metamorphic Suite|50425|6|Mentioned|p2.1, 4.1|||||||||
27277|Morrissey Metamorphic Suite|50542|6|Mentioned|p99, p104|Paleoproterozoic|Paleoproterozoic|Composed mainly of metasedimentary rocks that have been extensively migmatized. Also host to numerous Palaeoproterozoic granite intrusions. Geological Province: Gascoyne Region.||||||07-FEB-11
27277|Morrissey Metamorphic Suite|61262|5|Briefly described|p446, p454|||Previously contained Pooranoo Metamorphics (Williams et al, 1983 and Williams, 1986). At least 3 sedimentary packages (recent SHRIMP): Pooranoo, and Moogie Metamorphics, and metasedimentary rocks in Limejuice Zone. See also "Morrissey Metamorphic Suite".||||||18-JAN-07
27277|Morrissey Metamorphic Suite|63469|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Comprises pelitic schist and gneiss; musc-qtz-biot-plag-garnet-iron-oxide, staurolitie-muscovite-biotite-quartz rock and qtz-musc-biot-plag schist.||||||07-NOV-08
27277|Morrissey Metamorphic Suite|63866|5|Briefly described|p156|||Obsolete name for schists and gneisses now included in the Halfway Gneiss.||||||
27277|Morrissey Metamorphic Suite|63869|5|Briefly described|p16|||Williams et al.(1983); Williams (1986). Gascoyne Complex. Many components are separated by major faults or shear zones and large areas of granite; metasedimentary rocks have a large range of depositional ages and constitute several discrete packages. One such is the newly named Pooranoo Metamorphics.|||||A suite of metamorphosed and deformed sedimentary and minor igneous rocks thought to form a single supracrustal sequence.|
27277|Morrissey Metamorphic Suite|64384|5|Briefly described|p77, p81 Fig. 89iii|||Medium- to high metamorphic rocks of the Gascoyne Complex.||||||07-FEB-11
27277|Morrissey Metamorphic Suite|66299|6|Mentioned|pp3-5, p95, p121.|||Superseded name for rocks now packaged as Moogie Metamorphics, Camel Hills Metamorphics, Leake Spring Metamorphics and Pooranoo Metamorphics. This Suite was thought to outcrop throughout Gascoyne Province and to be equivalent to the Wyloo Group to the north, and sedimentary rocks of the Yerrida and Bryah Groups to the east. There is, however, no certainty that all these metasedimentary rocks were deposited in the same basin or are the same age. ||||||
27277|Morrissey Metamorphic Suite|67855|5|Briefly described|p199 fig 3-2, p201, p202, 222, 223|||||Gascoyne Complex||||
27277|Morrissey Metamorphic Suite|72758|5|Briefly described|p4 Fig.1, p9-12 Tb.1, p43-45, p58, p60.|||Gascoyne Province. Anatexis of this suite is possibly the mechanism for the formation of the Kilba Granite unit. Shown as including Mudong Metamorphics on p11, but text p44-45 does not support this relationship.  See also Morrissey Metamorphics p58.||||Unconformably underlies Wongida Dolomite Member.|Includes rocks ranging in metamorphic grade from quartz muscovite schist through biotite-muscovite-quartz-feldspar gneiss to an assemblage of quartz-muscovite-biotite schist interfoliated with bands of tourmaline granitoid and pegmatoid.|
38125|Morrissey Metamorphic Suite""|23525|5|Briefly described|p8|||Superseded name - see Morrissey Metamorphic Suite.   Now included in the Moogie Metamorphics and Camel Hills Metamorphics.||||||
38125|Morrissey Metamorphic Suite""|61262|6|Mentioned|p444|||Informal - see Morrissey Metamorphic Suite. Medium- to high-grade metasedimentary rocks of the Gascoyne Complex which grade northwards into lower grade metasedimentary rocks of the Upper Wyloo Group, in particular the Ashburton Formation.||||||18-JAN-07
38125|Morrissey Metamorphic Suite""|66950|6|Mentioned|p3, p4, p7|||Williams (1978). Gascoyne Province. Replaced by the "Morrissey Metamorphics" and subsequently the Leake Spring Metamorphics. These rocks have been reassigned to either the older Moogie Metamorphics and Camel Hills Metamorphics, or to the younger Pooranoo Metamorphics (e.g. Occhipinti and Sheppard, 2001; Martin et al., 2005, 2007).||||||16-DEC-16
78654|Morrissey Metamorphics""|66950|6|Mentioned|p7|||Originally the "Morrissey Metamorphic Suite" (Williams et al. 1978, 1983; Williams, 1986). Replaced by the Leake Spring Metamorphics. Most of what was thought to be "Morrissey Metamorphics", including the type areas for the original "Morrissey Metamorphic Suite"(Williams et al., 1978), has been reassigned to either the older Moogie Metamorphics and Camel Hills Metamorphics, or to the younger Pooranoo Metamorphics (e.g. Occhipinti and Sheppard, 2001; Martin et al., 2005, 2007).||||||16-DEC-16
28779|Mosquito Creek "Series"|31901|6|Mentioned|p238|||||||||
28779|Mosquito Creek "Series"|39426|6|Mentioned|Table 1|||||||||
28779|Mosquito Creek "Series"|48826|14|Not recorded|p.13|||Ref.to Reeves,1949.||||||
28780|Mosquito Creek Group""|39697|6|Mentioned|p18|||||||||
77948|Mosquito Well Conglomerate|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Stated to be a unit within Vivien Formation [in which case it must have Member appended].|2690 - 2660 Ma (inferred).|Vivien Formation|||Conglomerate with interbedded sandstone; common mafic clasts; metamorphosed.|
77948|Mosquito Well Conglomerate|70326|5|Briefly described|p339|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Vivien Formation.||Underlain unconformably by Turret Dolerite.||
77948|Mosquito Well Conglomerate|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2692-2662 Ma (inferred)|Unit of Mount White Group.|||Conglomerate with interbedded sandstone; common mafic clasts; metamorphosed|
78678|Mougoodera Formation|24160|5|Briefly described|p112.|||||Unit in Mount Farmer Group.||Unconformably overlies Luke Creek Group.|Upward-fining sequence of clastic sedimentary rocks.|
79803|Mougouderra Formation|70419|6|Mentioned|p2|||Murchison Domain, Youanmi Terrane, Yilgarn Craton.||||||
79803|Mougouderra Formation|70830|5|Briefly described|p58||||<2746 Ma|||||
73866|Mount Ada Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Basalt and chert. Thickness: 2km. Mount is Mt in text of Table. Geological Province: Pilbara Craton.||||||07-FEB-11
73866|Mount Ada Formation|24590|5|Briefly described|p196|Archean|Archean|Misspelt? See Mount Ada Basalt. Age: 3469+/-3Ma.||||||07-FEB-11
73866|Mount Ada Formation|60636|6|Mentioned|p35-36 Fig. 3.2|||Of the Warrawoona Group. Presented as Mt Ada  in text of figure. Name used interchangeably with Mount Ada Basalt.||||||07-FEB-11
73866|Mount Ada Formation|62427|5|Briefly described|p3 Fig.2, p4, p10 Fig.6|Paleoarchean|Paleoarchean|See also references to [the formal unit] Mount Ada Basalt (p4, p15). Age inferred from Fig.9.|3469 +/- 3 Ma.|Of the Warrawoona Group|||Mainly basalt.|
73866|Mount Ada Formation|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
73866|Mount Ada Formation|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.47 Ga.|Warrawoona Group.||||
32821|Mount Anderson Formation|48826|14|Not recorded|p.36,37|||May be present in NE Canning Basin. Known only from drill holes. U.Carb.||||||
41362|Mount Andrew Migmatite Complex|50434|6|Mentioned|p2.2|||||||||
27202|Mount Andrew Migmatites|30562|2|Defined|p17|Proterozoic|Proterozoic|See also P7.||||||
27202|Mount Andrew Migmatites|30563|6|Mentioned|p9|||Refers Doepel (in press)||||||
27202|Mount Andrew Migmatites|30959|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
39439|Mount Angelo Porphyry|22754|5|Briefly described|p20|||||||||
39439|Mount Angelo Porphyry|24572|6|Mentioned|Map - list|||Geological Province: Halls Creek Orogen.||||||
70438|Mount Barker Stone|61273|5|Briefly described|p85|Eocene|Eocene|Not intended as a formal name. Commercial name for dimension stone quarried from the pallinup Formation near Mount Barker. Spongolite - a pale brown, porus rock. Geological Province: Bremer Basin.||||||17-MAY-06
67873|Mount Barren Formation|60076|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|At margin of the Yilgarn Craton.||||||
36946|Mount Belches Beds|9766|5|Briefly described|Map Legend|Archaean|Archaean|Biotite-bearing metasedimentary rocks derived from turbidite, minor felsic volcaniclastic sedimentary rock.||||||
36946|Mount Belches Beds|23584|6|Mentioned|p4|||Renamed Mount Belches Formation. Geological Province: Yilgarn Craton.||||||
36947|Mount Belches Beds""|23584|6|Mentioned|p3|||Replaced by Mount Belches Formation. Geological Province: Yilgarn Craton.||||||
38645|Mount Belches Sandstone|23786|5|Briefly described|p5|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
38645|Mount Belches Sandstone|60555|6|Mentioned|p6 Fig. 3|Archean|Archean|Age: <2666+/-5Ma (Krapez et al., 2000).||||||07-NOV-08
38645|Mount Belches Sandstone|64633|6|Mentioned|p6 Fig.4.|||Kurnalpi Terrane. Appears in text as Mt Belches Sandstone.|<2666 +/- 5 Ma (Krapez et al. 2000).|||||
38645|Mount Belches Sandstone|66880|6|Mentioned|p8 Fig.2. |Archean|Archean||2666 +/- 5 Ma (Krapez et al. 2000).|||||
38645|Mount Belches Sandstone|72049|6|Mentioned|p257, p259|||Geochronology analyses, results, and interpretation are discussed in detail.||Kurrawang Group||||
77534|Mount Belches Sequence|66880|6|Mentioned|p10. |Archean|Archean|Gindalbie Terrane. See also Mount Belches sandstone, Table 1. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank.||||||01-NOV-12
32736|Mount Belches greywacke|23584|6|Mentioned|p37 Appendix 2|||Replaced with Mount Belches Formation. Geological Province: Yilgarn Craton.||||||
32736|Mount Belches greywacke|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
38657|Mount Belches sandstone|23786|5|Briefly described|p27|||Informal name - see Mount Belches Sandstone.  Geological Province: Yilgarn Craton.||||||
40408|Mount Boggola Volcanics|24607|5|Briefly described|p971 Fig. 6|Paleoproterozoic|Paleoproterozoic|Accidental formalisation of the Mount Boggola volcanic succession, of the Ashburton Formation. Age: 1829 +/- 5 Ma (U-Pb SHRIMP) is probably of volcaniclastic material, where detritus not transported far from source, so the age is considered to represent a younger limit on Mount Boggola volcanic succession in the Ashburton Formation. See also p969, where age is given as 1828+/-5 Ma. Geological Province: Ashburton Basin. See discussion p970-973||||||17-OCT-16
40451|Mount Boggola volcanics|24602|6|Mentioned|p861 Fig. 4|||Mount is Mt. in text of figure. Geological Province: Ashburton Fold Belt.||||||
41120|Mount Boreas granitoid complex|24196|6|Mentioned|p49|||||||||
28788|Mount Brown Ash Flow Tuff|32189|6|Mentioned|Fig.1|||||||||
76139|Mount Bruce Megasequence|65825|6|Mentioned|p20.|Archean|Archean|Term used by Blake and Barley (1992) for Mount Bruce Supergroup.||||||
39758|Mount Cassiterite pegmatite|24193|5|Briefly described|p887|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38613|Mount Cassiterite pegmatite group|23784|4|Described|p47|Archean|Archean|Not a stratigraphic name.||||||07-NOV-08
38613|Mount Cassiterite pegmatite group|24193|4|Described|p885|Archean|Archean|Geological Province: Pilbara Craton. Informal - see also Mount Cassiterite Pegmatite Group.||||||07-NOV-08
38613|Mount Cassiterite pegmatite group|50542|5|Briefly described|p110, p111|||Informal name.Pegmatites form a series of stacked tantalum-rich sheets intruding fine-grained, psammitic metasedimentary rocks with a minor pelitic biotite interbeds in the central-southern part of the Wodgina area. Geol Prov: Pilbara Craton.||||||07-FEB-11
34200|Mount Charlotte Scheelites|22645|6|Mentioned|Fig8 P211|||Mount actually spelt Mt||||||
40329|Mount Charlotte scheelite|23924|5|Briefly described|p205|Archean|Archean|Geological Province: Yilgarn Craton.  Age: 2772 +/- 82 Ma (Sm/Nd).  Mount is Mt. in text.||||||07-NOV-08
22403|Mount Christine Granitoid|22754|5|Briefly described|p7, p8|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite.  Age: c. 1808 Ma.  See also p11.||||||07-NOV-08
22403|Mount Christine Granitoid|23323|5|Briefly described|p456 Table 1, p462 Fig. 10|Orosirian|Orosirian|Age: 1808 +/- 3 Ma. Mount is Mt in text.||||||07-FEB-07
22403|Mount Christine Granitoid|23383|4|Described|p15, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite (Lamboo Complex).  Mainly composed of medium- to coarse-grained biotite monzogranite and hronblende-biotite monzogranite and granodiorite.  Intrudes Tickalara Metamorphics.   Age: 1820-1805Ma.  Geol.Prov: Halls Creek Orogen.||||||07-NOV-08
22403|Mount Christine Granitoid|23599|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Age: 1819+/-4 Ma, to 1808+/-3Ma (SHRIMP U-Pb zircon). Of Sally Downs supersuite.||||||07-NOV-08
22403|Mount Christine Granitoid|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex.  Coarsely porphyritic medium-grained biotite monzogranite.  Age: 1820Ma.||||||07-NOV-08
22403|Mount Christine Granitoid|23925|5|Briefly described|p221 Table 1|Orosirian|Orosirian|Age: 1808 +/- 3 Ma. Geological Province: Halls Creek Orogen.||||||
22403|Mount Christine Granitoid|24173|5|Briefly described|p15, 18|Paleoproterozoic|Paleoproterozoic|Age: 1808 +/- 3Ma and 1819 +/- 4Ma (AGSO/OZCHRON). Intrudes the Halls Creek Group||||||07-NOV-08
22403|Mount Christine Granitoid|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
22403|Mount Christine Granitoid|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite. Coarsely porphyritic to medium-grained biotite monzogranite. Age: 1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
22403|Mount Christine Granitoid|44693|5|Briefly described|Map Legend||Proterozoic|||||||
22403|Mount Christine Granitoid|44694|5|Briefly described|Map Legend||Proterozoic|||||||
22403|Mount Christine Granitoid|50437|5|Briefly described|p1.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Sally Downs Supersuite. Used interchangeably with Mount Christine Granite.||||||07-NOV-08
22403|Mount Christine Granitoid|63866|5|Briefly described|p129-p130, p132, p138|||Eastern Zone, Halls Creek Orogen. Mistakenly referred to as the Mount Christie Granitoid on p138.|c 1817-1808 Ma|Sally Downs Supersuite||||
22403|Mount Christine Granitoid|66845|4|Described|p537 Fig.3, p539 Tb.1, p542, p543 Fig.9|||Presented as Mt. Christine Granitoid. Mount Christine Granitoid (older and younger portions) are assigned to two different parents (Syenite Camp Suite and Kevins Dam suite, respectively) in Tb1. SHRIMP U-Pb zircon dating results. 1808+/-3 Ma regarded as magmatic age for this unit (16 analysed points); 1 other analysed point aberrantly young and discordant. Suggests two intrusive phases about 10 million years apart.|1817+/-4 (older), 1808+/-3Ma (younger) SHRIMP U-Pb|Syenite Camp suite and Kevins Dam suite|||older (foliated granodiorite); younger (biotite monzogranite)|
22403|Mount Christine Granitoid|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1808 Ma|Of Kevins Dam suite.||||
22403|Mount Christine Granitoid|71267|6|Mentioned|1M_geologyp12_lut.csv|||See Mount Christine Granite. |||||Medium- to coarse-grained biotite monzogranite and hornblende-biotite monzogranite and granodiorite.|
22403|Mount Christine Granitoid|72437|5|Briefly described|p102-104|||Whole rock analyses are provided.||Kevins Dam Suite|||Biotite monzogranite, porphyritic biotite monzogranite, fine-grained biotite monzogranite.|
77407|Mount Christine Monzogranite|65413|6|Mentioned|p107.|Paleoproterozoic|Paleoproterozoic|Southern Halls Creek Orogen.|1810 Ma.|||||
68127|Mount Clifford greenstones|60416|6|Mentioned|p5|||Informal name.  Within the Mount Clifford greenstone belt which extends across the entire LEONORA sheet.||||||
37155|Mount Crofton Granite "Complex"|23760|5|Briefly described|p39|Neoproterozoic|Neoproterozoic|Age: 598+/-24 Ma (Rb-Sr). Informal.||||||
40182|Mount Crofton Granite "complex"|24594|5|Briefly described|p608 Fig. 4|Neoproterozoic|Mesoproterozoic|Age: ~560-650Ma (Rb-Sr isochron, Trendall 1974).  Geological Province: Paterson Orogen.||||||
41439|Mount Crofton Group|50436|5|Briefly described|p4.1|Neoproterozoic|Neoproterozoic|Includes: Mount Crofton Granite, Hansens Folly Granite, Desert's Revenge Granite. Of the O'Callaghans Supersuite. Geological Province: Paterson Orogen.||||||10-AUG-04
74160|Mount Crofton Suite|24197|5|Briefly described|p100, 101|||One of two suites in O'Callaghans Supersuite - oxidised; the other is O'Callaghans Suite (reduced).||||||27-SEP-12
74160|Mount Crofton Suite|65454|5|Briefly described|p12|Cryogenian|Cryogenian|Of O'Callaghans Supersuite. Oxidised and magnetite-bearing, highly fractionated, I-type. Forms magnetic highs.||||||
74160|Mount Crofton Suite|67202|4|Described|p55 Fig.3.4, p57, p60, p63,p128,p190-191|||See also p221, p254, p256, p259, p261. Wyborn (1997) and Budd et al. (2001). Also appears as Mount Crofton Granite Suite on p57, p63, p221, p224, p254, p256, p259, p261 and Mount Crofton Granite suite on p6. Plutons trend NE. Source of uranium and vanadium.|650-630 Ma (SHRIMP U-Pb).|O'Callaghans Supersuite.|Mount Crofton Granite.|Intrudes Lamil Group.|Granitoids and minor coeval volcaniclastics.|15-FEB-18
74160|Mount Crofton Suite|68902|6|Mentioned|p5 fig 3, p7|Neoproterozoic|Neoproterozoic|Also called Mount Crofton Granite||||||
41122|Mount Dennis granitoid complex|24196|5|Briefly described|p49|Archean|Archean|Mount is Mt. in text. Age: migmatite 2770 +/- 5 Ma (Dunphy et al., in prep).||||||07-NOV-08
41121|Mount Dennis migmatite|24196|5|Briefly described|p50|Archean|Archean|Informal name. Referring to the migmatite of Mount Dennis granitoid complex. Age: 2770 +/- 5 Ma (Dunphy et al., in prep)||||||07-NOV-08
28794|Mount Dugel sequence|41942|6|Mentioned|p68|||||||||
72994|Mount Edgar Granitic Complex|63142|6|Mentioned|p487, p488|||||||||29-MAR-07
72994|Mount Edgar Granitic Complex|64405|5|Briefly described|p2 Fig. 1|||||||||07-FEB-11
72994|Mount Edgar Granitic Complex|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Undivided granitic rock; metamorphosed.||||||15-DEC-08
72994|Mount Edgar Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
72994|Mount Edgar Granitic Complex|65827|3|Fully described|p1, p9 Fig 3, p10, p14-16, p18-33, p40|Mesoarchean|Paleoarchean|Griffin (1990); Williams (1999); formerly Mount Edgar Batholith or Mount Edgar Igneous Complex. Includes Callina, Tambina, Emu Pool, Cleland and Split Rock Supersuites. Unconformably underlies Mount Roe Basalt, Fortescue Group.  Intruded by Moolyella Monzogranite, Black Range Dolerite Suite. Intrusion c.3315-3290 Ma and renewed 3246-3241 Ma.||||||
72994|Mount Edgar Granitic Complex|65829|6|Mentioned|p26.|||Apparently is associated with exposed ring faults, unlike the Fortescue Group in this map area.||||||
72994|Mount Edgar Granitic Complex|66217|4|Described|p1, pp8-9, p11, p16, p24, pp35-36, p59.|Paleoarchean|Paleoarchean|East Pilbara Terrane. 60 km diameter, circular complex. Several authors have proposed a diapiric model, involving multiple thermotectonic events, for the evolution of this Complex. Others also invoke Alpine-style thrusting. Wrapped-around by Marble Bar greenstone belt. Hosts alluvial Sn at Garden Creek, and porphyry copper-molybdenum mineralisation.|c.3300 Ma.||Includes elements of  Emu Pool, Callina, Tambina, Cleland and Split Rock Supersuites.|Intrudes and includes enclaves of North Star Basalt.||18-DEC-12
72994|Mount Edgar Granitic Complex|67197|6|Mentioned|p3|||East Pilbara Terrane.||||||
72994|Mount Edgar Granitic Complex|67270|6|Mentioned|p3|Archean|Archean|||||||
72994|Mount Edgar Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
72994|Mount Edgar Granitic Complex|68284|6|Mentioned|p5|||East Pilbara Terrane, Pilbara Craton.||||||
72994|Mount Edgar Granitic Complex|69167|6|Mentioned|178034.1.pdf|Archaean|Archaean|(Structural?) Age derived from sample of leucotonalite and biotite granodiorite (178100.1.pdf, 178037.1.pdf)|3435 +/- 3 Ma - 3313 +/- 2 Ma (SHRIMP)|||||
72994|Mount Edgar Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
72994|Mount Edgar Granitic Complex|70733|6|Mentioned|p105||`|Eastern Pilbara Craton.||||||
72994|Mount Edgar Granitic Complex|73598|6|Mentioned|p1208 Fig.1|||East Pilbara Terrane. Appears as Mount Edgar Granite Complex.||||||
33902|Mount Edgar Granitoid Complex|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3310 Ma||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|22715|5|Briefly described|p216|Archean|Archean|Spelt "Mt" in the text. Age: approx 3315-3310Ma||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|22906|6|Mentioned|p46|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|23585|6|Mentioned|p12|Archean|Archean|||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|23755|6|Mentioned|p9|||||||||
33902|Mount Edgar Granitoid Complex|23783|5|Briefly described|p17|Archean|Archean|||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|23784|5|Briefly described|p70|Archean|Archean|||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|23807|6|Mentioned|p108|||Geological Province: Pilbara Craton.  Mount is Mt in text.||||||
33902|Mount Edgar Granitoid Complex|23813|5|Briefly described|p103|Archean|Archean|Mount is Mt. in text.  Geological Province: Pilbara Craton.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|23895|5|Briefly described|p884 Fig.1, p904|||Mount is Mt in text.  Geological Province: Pilbara Craton.||||||07-MAR-05
33902|Mount Edgar Granitoid Complex|23936|6|Mentioned|p16|||Mount is Mt in text. Geological Province: Pilbara Craton.||||||
33902|Mount Edgar Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3466-2830Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|24184|4|Described|p703, p707 Fig.8|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3450Ma||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|24531|6|Mentioned|p39|||||||||
33902|Mount Edgar Granitoid Complex|24550|5|Briefly described|p32, p53 Fig. 4.4|Archean|Archean|Age: ca 3300Ma. Referred to as the 'ca 3300-3320 granite suite'. See also p55.||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|24590|5|Briefly described|p16, p32|Archean|Archean|Dominated by trondhjemite-tonalite-granodiorite intrusions geochemically divided into 6 suites. Two of these are: Coppin Gap and Boodallan Suites. Age : 3.32-3.31Ga. Mount is Mt in text. See also p41.||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|44150|5|Briefly described|p129, p130-131 Fig.2-130, p142|||See also p144-145 Tb.2-21, p150 Fig.2-138, p152, p153 Fig.2-140, p155 Fig.2-142. Intrusive in the north, tectonic in the south. Various ages given, ranging 3280 - 2614 Ma.|||Includes Moolyella Adamellite.||Monzogranites, granodiorites, syenogranite, gneiss, greenstones.|
33902|Mount Edgar Granitoid Complex|44229|5|Briefly described|Map legend|Archean|Archean|Metamorphosed medium- to coarse-grained monzogranite, granodiorite, tonalite, and trondjhemite; massive, seriate, and porphyritic varieties; weakly foliated.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|50189|4|Described|p14, 22|Archean|Archean|Of the Mount Edgar Batholith. Includes four coalescing, bulbous-shaped plutons. See also p6 Fig. 3, p8 Fig. 4.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|50427|5|Briefly described|p174|Archean|Archean|||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|50544|4|Described|p30, p10 Fig. 5|Archean|Archean|In YARRIE this complex includes portions of the following plutons: Coppin Gap and Mullungunya Granodiorites, Munganbrina Monzogranite and Chimingadgi Trondhjemite.  Age: c.3460-2830Ma (Nelson, 2000; Williams and Collins, 1990; Williams, 1999a)||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Chimingadgi Trondhjemite, Coppin Gap and Mullugunya Granodiorites, and Munganbrina Monzogranite.  Age: 3460-3241Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|60429|4|Described|p6 Fig. 3, p14|Archean|Archean|Bulbous-shaped plutons of Munganbrina Monzogranite, Mullugunya Granodiorite, Coppin Gap Granodiorite and Chimingadgi Trondhjemite coalesce to form this complex. Age: c.3314Ma. Geological Province: Pilbara Craton. See also p8 Fig. 4.||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|60636|6|Mentioned|p11, p54|Archean|Archean|Includes the Coppin Gap Suite. Mount is Mt in text.||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|62427|6|Mentioned|p4-5, p14-16|||S of Coppin Gap Greenstone Belt.|||Includes Coppin Gap Suite.|||
33902|Mount Edgar Granitoid Complex|63866|5|Briefly described|p144|||Eastern Pilbara Granite-Greenstone Terrane.||||||
33902|Mount Edgar Granitoid Complex|64326|6|Mentioned|p71 Fig. 1|Archean|Archean|Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|64327|6|Mentioned|p62 Fig. 1|Archean|Archean|||||||07-NOV-08
33902|Mount Edgar Granitoid Complex|64328|6|Mentioned|p54, p58|||||||||07-FEB-11
33902|Mount Edgar Granitoid Complex|64936|5|Briefly described|map legend|Archean|Archean|Includes Coppin Gap Granodiorite and Munganbrina Monzogranite. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
33902|Mount Edgar Granitoid Complex|65008|6|Mentioned|p14, p15|||||||||
33902|Mount Edgar Granitoid Complex|65455|6|Mentioned|p5|Archean|Archean|Pilbara Craton.||||||09-MAY-12
33902|Mount Edgar Granitoid Complex|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Also includes Lady Adelaide Orthogneiss; Fig Tree, Underwood Gneisses, and Davitt Syenogranite; as well as three or four un-named but separately-mapped units.|c.3324 - 2831 Ma (Collins et al. 1998).||Includes Moolyella, Bishop Creek, Bullgarina, Munganbrina Monzogranites; Joorina, Mullugunya, Zulu, Coppin Gap, Chessman, Kennell, Wilina Granodiorites; Chimingadgi, Walgunya Trondjhemites.|Intruded by Apex Basalt.||
78451|Mount Edgar Igneous Complex|65827|6|Mentioned|p14|Mesoarchean|Paleoarchean|The name by which the Mount Edgar Granitic Complex is referred in Sims and Carson, 2001.||||||
78452|Mount Edgar Mylonite Complex|65827|6|Mentioned|p59, p60|Paleoarchean|Paleoarchean|Of Sims and Carson, 2001. Corresponds in part to Underwood Gneiss.||||||16-OCT-13
78452|Mount Edgar Mylonite Complex|69041|6|Mentioned|p18||||3061 +/- 357 Ma (Collins & Gray, 1990)|||||
32598|Mount Edgar Porphyrite|44297|14|Not recorded|p.13|||(F51-9).||||||
32598|Mount Edgar Porphyrite|45923|4|Described|p.88||Neoproterozoic|See also p66, 95.||||||
38969|Mount Edgar granitoid complex|23807|6|Mentioned|p137|||Informal - see Mount Edgar Granitoid Complex.  Geological Province: Pilbara Craton.||||||
38969|Mount Edgar granitoid complex|24193|5|Briefly described|p874 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38969|Mount Edgar granitoid complex|24590|6|Mentioned|p35, p132 Fig. 4.2|||Informal - see Mount Edgar Granitoid Complex. Mount is Mt in text.||||||07-FEB-11
38969|Mount Edgar granitoid complex|60636|6|Mentioned|p49|||Misspelt - see Mount Edgar Granitoid Complex.  Mount is MT in text.||||||07-FEB-11
83954|Mount Edwards Basalt|70863|6|Mentioned|p9, p11 Fig.7, p12|||Widgiemooltha Dome, Yilgarn Craton. Footwall to the Miitel komatiite-hosted Ni-Cu-(PGE) deposit. Presented in two of these mentions as Mount Edwards basalt.||||||
80174|Mount Eliza Formation|71211|6|Mentioned|p216|||||Mount Palgrave Group||||
81394|Mount Eliza granophyre|67553|6|Mentioned|p21 fig.11|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin.. Crystallisation age 1077+\-6 Ma by GSWA 174662.|1077+\-6 Ma|||||16-AUG-19
78642|Mount Ellis Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 4 unnamed subunits.||Pyroxenite; iron-rich quartz gabbro with granophyric segregations; gabbro; leucogabbro and plagioclase-rich gabbronorite; all metamorphosed.|06-AUG-15
78642|Mount Ellis Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Pyroxenite, iron-rich quartz gabbro with granophyric segregations, gabbro, leucogabbro and gabbronorite; metamorphosed.|
78642|Mount Ellis Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro, leucogabbro and plagioclase-rich gabbronorite; metamorphosed, iron-rich quartz gabbro with granophyric segragations; metamorphosed, pyroxenite; metamorphosed.|
32739|Mount Elma Conglomerate|44366|14|Not recorded|p.20|||||||||
32739|Mount Elma Conglomerate|44998|14|Not recorded|p26,32,33,43, map||Late Devonian|U.Devonian.||||||
32739|Mount Elma Conglomerate|66127|5|Briefly described|p134, p149.|||Of Guppy et al. (1958). Type locality at Mount Elma. Subsequently renamed Elma Conglomerate by Tyler et al. (1998) and this study.||||Interfingers with small patch reefs of Pillara Limestone.||
81398|Mount Eveline granite|67553|5|Briefly described|p21,40|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Also called Mount Eveline granite on 40. Similar in composition to Wururu Rhyolite, and coeval with high-level block-faulting (caldera subsidence) and emplaced at 1065-1063 Ma along faults.|1065-1053 Ma|||Correlable to Wururu Rhyolite.||
41461|Mount Fairbairn Granite|50437|6|Mentioned|p4.1|||Of the Syenite Camp Suite (Sally Downs Supersuite). Geological Province: Kimberley Region. Used interchangeably with Mount Fairbairn Monzogranite.||||||10-AUG-04
41461|Mount Fairbairn Granite|72437|5|Briefly described|p99-100|||Whole rock analyses are provided.||Syenite Camp Suite|||Biotite monzogranite, metadiorite, porphyritic biotite monzogranite.|
41363|Mount Franklin granite|50434|5|Briefly described|p3.1|Mesoproterozoic|Mesoproterozoic|Informal. Geological Province: Albany-Fraser Province. Of the Nornalup Supersuite. Age: 1189 +/- 9Ma (Shrimp).||||||
75930|Mount Gibson Group|67129|5|Briefly described|p18 Fig.19|Archean|Archean|Murchison Domain, Youanmi Terrane.|>2935 Ma.|Murchison Supergroup.||||
75930|Mount Gibson Group|68109|5|Briefly described|p659|Mesoarchean||Murchison Domain.|> 2900 Ma|Of the Murchison Supergroup.||||
75930|Mount Gibson Group|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Murchison Supergroup.|Includes Golden Grove and Orion formations.|Overlain (?disconformably) by Norie Group/Murrouli Basalt.||
75930|Mount Gibson Group|72494|5|Briefly described|p15|||Western Youanmi Terrane, Yilgarn Craton.|2960-2935 Ma.||||Intermediate and felsic volcanic units intercalated with chemical sedimentary rocks and overlain by volcaniclastic mass-flow units and BIFs.|
83876|Mount Gibson banded iron formation|69267|5|Briefly described|p651-652, 654, 658, 660, 663|||Murchison Province, Yilgarn Craton. Petrography, geochemistry described in great detail. Appears as Mount Gibson BIF after initial appearance.||Windanning Formation.|||Alternating bands of magnetite and microcrystalline quartz (chert) with rare carbonaceous and iron silicate-rich shale partings and rare tuff bands. c.100m thick.|
80244|Mount Goode basalt|70276|6|Mentioned|p783|||Mount Keith area, Agnew-Wiluna greenstone belt, Yilgarn Craton. Mineralised.|||||Tholeiitic basalt.|
80244|Mount Goode basalt|71310|5|Briefly described|p778-780, p784|||Kathleen Valley-Yankabindie district. Faces E; is overturned. Deformation described.||||||
74057|Mount Goodwin Formation, Lower|13222|6|Mentioned|p229 Fig.2, p231 Fig.4.|||See Mount Goodwin Formation.||Unit in Kinmore Group.||||
74057|Mount Goodwin Formation, Lower|13242|3|Fully described|p214 Fig. 2, p226 Fig. 8|Early Triassic|Early Triassic|Informal division of Mount Goodwin Formation. Conformable over Penguin Formation. Geological Province: Bonaparte Basin. Detailed lithology included.||||||07-FEB-11
74057|Mount Goodwin Formation, Lower|64690|5|Briefly described|p504 Fig.2 |Early Triassic|Early Triassic|See also reference to Mount Goodwin Formation (p505).||||Overlies Penguin Formation. Is overlain by Upper Mount Goodwin Formation.||
74057|Mount Goodwin Formation, Lower|64692|6|Mentioned|p522 Fig.2 |Early Triassic|Early Triassic|Bonaparte Basin.||||Overlies Penguin Formation. Is overlain by Upper Mount Goodwin Formation.||
74057|Mount Goodwin Formation, Lower|69452|6|Mentioned|p36:21|||Gorter (1998); Gorter et al. (2009). Now the Mairmull Formation.||||||12-JUL-16
74057|Mount Goodwin Formation, Lower|71623|6|Mentioned|p345 fig 2, p353 Fig 11||Scythian|Bonaparte Basin|||||Shale|
74058|Mount Goodwin Formation, Upper|13222|6|Mentioned|p229 Fig.2, p231 Fig.4.|||See Mount Goodwin Formation.||Unit in Kinmore Group.||||
74058|Mount Goodwin Formation, Upper|13242|3|Fully described|p214 Fig. 2, p224-225|Early Triassic|Early Triassic|Informal division of Mount Goodwin Fm. Unconformable below Cape Londonderry Fm (Timor Sea )and below Osprey Fm. Geol.Prov: Bonaparte Basin.Comprises grey + green claystones + minor siltstone + sandstone (detailed lithology included).||||||07-FEB-11
74058|Mount Goodwin Formation, Upper|64690|6|Mentioned|p504 Fig.2|Early Triassic|Early Triassic|See also reference to Mount Goodwin Formation (p505).||||Overlies Lower Mount Goodwin Formation. Is overlain by Cape Londonderry Formation.||
74058|Mount Goodwin Formation, Upper|64692|6|Mentioned|p522 Fig.2 |Early Triassic|Early Triassic|Bonaparte Basin.||||Overlies Lower Mount Goodwin Formation. Is overlain by Cape Londonderry Formation.||
73995|Mount Goodwin Shale|14227|5|Briefly described|p10|Triassic|Triassic|Geological Province: Bonaparte Basin. Mount is Mt in text.||||||07-FEB-11
77460|Mount Goodwin Sub-group|67370|1|Redefined|p313, pp316-318, pp332-333.|Early Triassic|Late Permian|Redefined as a Subgroup in this study. Originally Mount Goodwin Formation of Helby (1974); redefined by Mory (1988); informally divided into Lower and Upper units (Gorter 1998). The base of this unit is an unconformity overlying older Permian strata. The top of this unit is an erosional surface below the Osprey Formation (eastern Bonaparte Basin) and Sahul Group (western Bonaparte, northern Browse Basins). Shallow marine to paralic. The several hundred metres of sediments were deposited in 1 - 1.5 million years, possibly dispersed by wind.||Upper unit in Kinmore Group.|Includes (at the base) Penguin, Mairmull, Ascalon and (at the top) Fishburn Formations.|Overlies Tern Formation and Hyland Bay Subgroup. Is overlain by Osprey Formation.|Mainly siltstones.|
77460|Mount Goodwin Sub-group|69653|6|Mentioned|p10|Triassic|Triassic|Petrel Sub-basin.||Kinmore Group.|Mairmull, Ascalon, Fishburn Formations.|Overlies Hyland Bay Sub-group. Is overlain by Lower Cape Londonderry Formation.||
77460|Mount Goodwin Sub-group|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||Is overlain by Nome Formation.||
77460|Mount Goodwin Sub-group|70064|5|Briefly described|Regional Fig. 6|Early Triassic|Early Triassic|Prudhoe Terrace, Browse Basin.||Kinmore Group.||Overlies Hyland Bay Subgroup. Is overlain by Sahul Group.||12-JUL-16
39761|Mount Hall pegmatite group|24193|5|Briefly described|p875, Fig.2, p888|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
37205|Mount Hall-Carlow Castle Complex""|23793|6|Mentioned|p29|||Renamed Andover Intrusion||||||
32820|Mount Hardman beds|48826|14|Not recorded|Not recorded|||Tb.III. Correlates with Hardman Member. (Name should not be perpetuated; Hardman Member is sufficient.)||||||
32820|Mount Hardman beds|48831|14|Not recorded|p.69|||||||||
26762|Mount House Beds|39796|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26762|Mount House Beds|44363|14|Not recorded|p.12,13|||Unconformably overlies Bastion group.||||||
26762|Mount House Beds|44998|14|Not recorded|p17,21|||||||||
26762|Mount House Beds|45022|6|Mentioned|p86|||||||||
26762|Mount House Beds|45102|6|Mentioned|p49|||||||||
26762|Mount House Beds|45923|14|Not recorded|p.72|||||||||
23820|Mount James Beds|36551|6|Mentioned|p95|||||||||
23820|Mount James Beds|38978|6|Mentioned|p149|||||||||
27206|Mount James Formation|22904|6|Mentioned|p57 fig 1|||||||||16-JUL-08
27206|Mount James Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27206|Mount James Formation|23485|4|Described|p24|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27206|Mount James Formation|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27206|Mount James Formation|23525|4|Described|p24||Statherian|Age: <1800Ma.||||||
27206|Mount James Formation|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27206|Mount James Formation|23780|5|Briefly described|p24|Orosirian|Orosirian|Underlain by Gascoyne Complex (unconformable).||||||18-JAN-07
27206|Mount James Formation|23781|5|Briefly described|p62|Paleoproterozoic|Paleoproterozoic|Age: c.1800Ma.||||||07-NOV-08
27206|Mount James Formation|24410|5|Briefly described|p137 Fig. 80|Proterozoic|Proterozoic|Of the Edmund Group? Metamorphosed conglomerate, sandstone, chert, siltstone, and mudstone. ||||||
27206|Mount James Formation|24544|4|Described|p3, 38|Paleoproterozoic|Paleoproterozoic|Age: 1800-1640 Ma. Quartzite, meta-arkosic sandstone to quartz-sericite phyllite, meta-quartz and metapolymict conglomerate, phyllite. Unconformably overlies Coor-de-wandy Fm., Halfway Gneiss, Moogie Meta's. Unconformably overlain by Bangemall Supergroup.||||||07-NOV-08
27206|Mount James Formation|24602|6|Mentioned|p862 Fig. 5|||||||||
27206|Mount James Formation|36902|6|Mentioned|Table 5|||||||||
27206|Mount James Formation|37299|6|Mentioned|Fig.1|||||||||
27206|Mount James Formation|39370|2|Defined|p28|Proterozoic|Proterozoic|||||||
27206|Mount James Formation|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27206|Mount James Formation|40937|5|Briefly described|p5|||||||||
27206|Mount James Formation|40938|6|Mentioned|p5|||||||||
27206|Mount James Formation|41360|6|Mentioned|p192|||||||||
27206|Mount James Formation|43255|5|Briefly described|map legend||Proterozoic|||||||
27206|Mount James Formation|43256|4|Described|5,15||Proterozoic|||||||24-NOV-09
27206|Mount James Formation|44142|6|Mentioned|p325, p327 Tb.4-5, p329|||Occurs in narrow, faulted troughs in GLENBURGH and MOUNT PHILLIPS map areas, where they are covered by Bangemall Group correlates.||||Is overlain unconformably by Ullawarra Formation.||13-MAR-18
27206|Mount James Formation|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27206|Mount James Formation|50216|5|Briefly described|p209|Paleoproterozoic|Paleoproterozoic|Detrital zircons range: 3300 to 1800 Ma, with prominent peaks at 2800-2650, 2000 and 1800 Ma.||||||07-NOV-08
27206|Mount James Formation|50218|5|Briefly described|p238 Fig. 1|Paleoproterozoic|Paleoproterozoic|Metasiliciclastic rocks. Age: <1800Ma. Geological Province: Errabiddy Shear Zone. See also Figs. 2 and 3, p240-41. Not Edmund Gp||||||07-FEB-11
27206|Mount James Formation|50219|5|Briefly described|p258 Fig. 1|Paleoproterozoic|Paleoproterozoic|Metasiliciclastic rocks.  Age: <1800Ma.  See also p260 Fig.2.||||||07-FEB-11
27206|Mount James Formation|50220|5|Briefly described|p281 Fig.1|||||||||
27206|Mount James Formation|50225|6|Mentioned|p388|||Unconformably overlain in part by Bangemall Supergroup rocks.||||||07-FEB-11
27206|Mount James Formation|61262|5|Briefly described|p455|Paleoproterozoic|Paleoproterozoic|Siliciclastic rocks. Unconformably overlies the Glenburgh Terrane in southern Gascoyne Complex. Mount is MT in text. ||||||07-NOV-08
27206|Mount James Formation|63246|6|Mentioned|p479, p480|||Low grade metasedimentary rocks. See also p490.||||||
27206|Mount James Formation|63866|5|Briefly described|p152, p155, p157-p159, p175|||SHRIMP U-Pb age is interpreted as the maximum age for deposition of this formation.|1801 +/- 13 Ma (Nelson, 2001)|||Unconformably overlain by the Edmund Group. Unconformably overlies the Coor-de-wandy Formation.|Quartzites.|
27206|Mount James Formation|65152|5|Briefly described|p3.|Paleoproterozoic|Paleoproterozoic|Basal unit in Pooranoo Metamorphics. Fluvial conglomerate and sandstone, and shallow-marine sandstone.||||||01-MAY-15
27206|Mount James Formation|65830|6|Mentioned|p26, p35 Fig.21, p39, Plate 2|||Rocks near Reid Well mapped by Williams et al. (1983) have been transferred to Pooranoo Metamorphics. Lithologically similar and has similar field relationships to the Pooranoo Metamorphics; possible correlatives.||||Possible correlative of the Pooranoo Metamorphics.||
27206|Mount James Formation|66299|6|Mentioned|p3, p215.|Paleoproterozoic|Paleoproterozoic|Superseded (as stated in the text) by Mount James Subgroup.||||||
27206|Mount James Formation|66950|6|Mentioned|p12|||Replaced by the Mount James Subgroup. Elevated to Subgroup status with the recognition of a coherent stratigraphy, and the identification of two internal formations (Spring Camp Formation and Biddenew Formation; Sheppard et al., 2008, 2010).||||||16-DEC-16
27206|Mount James Formation|67855|4|Described|p221-3, p197|Mesoproterozoic|Paleoproterozoic|Age poorly constrained. Type location: between Mt Gascoyne (24o57'25'' S 116o38'58") and Spring Outcamp (24o54'50",116o34'50"). Metamorphism, folding & cleavage development post-dates Morrisey Metamorphic Suite. 2km thick  sequence in ascending order: polymictic boulder conglomerate, well-bedded sandstone, massive quartz sandstone. ||||Unconformably overlies Gascoyne Complex rocks. Overlain by Bangemall Group unconformably. Correlated with Padbury Group, Mount Minnie Group, Capricorn Formation.|Metasediments include faintly banded ferruginous chert and graphitic phyllite overlain by green micaceous metasiltstone interbedded with quartzitic metasandstone.|
27206|Mount James Formation|69166|6|Mentioned|168937.1.pdf|Paleoproterozoic|Paleoproterozoic||||||Quartzite with minor muscovite and trace tourmaline, rutile and zircon.|
27206|Mount James Formation|70795|6|Mentioned|168937.1.pdf||||||||White, flaggy quarzite, coarse grained sandstone.|
27206|Mount James Formation|72259|6|Mentioned|App. Tb.B|||||||||
83269|Mount James Supergroup|72259|6|Mentioned|App. Tb.B||||||||Includes sandstone and conglomerate.|
42484|Mount James formation|50216|5|Briefly described|p209|||Informal - see Mount James Formation. Deformed and outcropping metamorphosed siliclastic rocks that outcrop in isolated strips through the Gascoyne Complex.||||||
79827|Mount James subgroup|69387|5|Briefly described|p23|||SG and magnetic susceptibility values given.||Pooranoo Metamorphics.|||Quartzite-dominated.|
33981|Mount John Member|22547|6|Mentioned|Fig4,p25|||Overlies Wade Creek Formation.||||||14-NOV-06
30212|Mount Jope Formation|43119|6|Mentioned|p7|||Variation of Mount Jope Volcanics?||||||15-AUG-05
30212|Mount Jope Formation|69745|6|Mentioned|p272|||Mount Wall area, Hamersley Province. Crops out immediately W of the Wellthandalthaluna Fe deposit.||Fortescue Group.|||Massive and pillowed lava flows, flow breccias and abundant dolerite sills.|
38089|Mount Jope Subgroup|23570|6|Mentioned|p237 Appendix 1|||Suggested alternative name for Mount Jope Volcanics but not introduced.||||||
39908|Mount Jope Volcanics""|24353|5|Briefly described|p26|Archean|Archean|Name no longer used. Redefined by Hickman (1983) as Maddina Formation. Geological Province: Pilbara Craton||||||07-NOV-08
73991|Mount Keith Dacite|63711|6|Mentioned|p863|||||||||
73991|Mount Keith Dacite|66192|6|Mentioned|p550, 551, 552|||Written Mt in text. In Agnew-Wiluna Greenstone Belt. With Centenary Bore Basalt, separates the underlying Mount Keith Ultramafic Unit and the overlying Cliff Ultramafic Unit; their combined thickness varies from 0 to c.800 m.||||||09-MAR-12
73991|Mount Keith Dacite|69414|6|Mentioned|p88|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton. Geochronology be M.Barley in Rosengren et al. (2008); Fiorentini et al. (2012).|2706 - 2713 +/- 6 Ma.|||||
73991|Mount Keith Dacite|70275|5|Briefly described|p471, 483|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.|2713 +/- 6 Ma; 2711 +/- 6 Ma.|||Overlies McFarlane's Basalt. Is overlain by Centenary Bore Basalt. Encloses Mount Keith Ultramafic Unit.|A sequence of dacitic rocks intercalated with very olivine-rich cumulate units.|
73991|Mount Keith Dacite|70276|5|Briefly described|p783-786|||Mount Keith Domain, Yilgarn Craton. Laterally extensive. Comprises multiple, tabular lava flows (some over 120m thick) with associated quench-fragmented and resedimented breccias (subaqueous).|2713 and 2711 +/- 6 Ma.|||Overlies MacFarlanes Basalt (nature of contact unknown). Is overlain by Centenary Bore Basalt. Abuts (probably intruded by) Mount Keith ultramafic unit.|Intermediate to felsic volcanic and locally volcaniclastic rocks.|
73991|Mount Keith Dacite|73596|6|Mentioned|p1151-1152, 1160, 1167|||Agnew-Wiluna Greenstone Belt. Rift-proximal felsic lava domes and cryptodomes.||||Paraconformably overlies Songvang Basalt. Is overlain by Agnew Komatiite.||
81381|Mount Keith Dunite|70326|6|Mentioned|p365|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton. See Mount Keith Ultramafic.|2713+/-6 Ma, 2706+/-6 Ma.|||||15-AUG-19
81380|Mount Keith Ultramafic|70326|5|Briefly described|p360,364|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton. [Also referred to as Mount Keith Dunite on p365]. Has been previously interpreted as a comagmatic intrusion to the extrusive Cliffs Ultramafc (Fiorentini et al., 2010). Contains dacites with crystallisation ages at 2713+\-6, 2706+\-6 Ma at the top of the sequence, and 2711+\-6 Ma at the bottom (U-Pb SHRIMP, Fiorentini et al., 2012). Correlable to Songvang Basalt.|c. 2710 Ma|||Overlain by Centenary Bore Basalt.||
34315|Mount Keith Ultramafic Complex|63711|4|Described|p848, p852, p854-5|||Part of Mount Keith Ultramafic unit. Assoc.with 2 other ultramafic horizons, Cliffs Ultramafic and Monument Ultramafic units. One of most highly nickel sulfide-endowed komatiite belts in world. Geol.Prov: Agnew-Wiluna Greenst. Belt. Mount is Mt in Figure.||||||15-JAN-08
34315|Mount Keith Ultramafic Complex|63712|5|Briefly described|p824, p827-828|||Part of Mount Keith Ultramafic unit; divided into 3 packages of units - main adcumulate domain, upper fractionated zone and western mineralised zone. Dunite body with komatiite affinities; lens/pods olivine accumulates. Geol.Prov: Agnew-Wiluna Greenst.Belt||||||28-MAR-13
34315|Mount Keith Ultramafic Complex|66192|6|Mentioned|p544, 548|||Written Mt in text.  In Mount Keith Ultramafic Unit.||||||09-MAR-12
34315|Mount Keith Ultramafic Complex|70863|6|Mentioned|p6, 9|||Yilgarn Craton. Exploration involved detecting crustal contamination by assimilation of fractionated material into the magma.||||||
75824|Mount Keith Ultramafic Unit|66192|5|Briefly described|p544, p545 Fig.2, p546, 548-549, 552|||Written Mt in text. In Agnew-Wiluna Greenstone Belt. Ni-mineralisation, 200-800m thick; gabbro meso/ortho cumulates are laterally extensive around pods and lenses of adcumulates; emplaced as an intrusive sill.||||||09-MAR-12
75824|Mount Keith Ultramafic Unit|70275|5|Briefly described|p471-472, 483, 488, 498|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton. A magmatic Re/Os age of 2706 +/- 36 Ma is reported by Rosengren et al. (2005). Also appears as Mt. Keith ultramafic unit.|2703 +/- 36 Ma.|||Is enclosed by Mount Keith Dacite.|A sequence of dacitic rocks intercalated with very olivine-rich cumulate units.|
75824|Mount Keith Ultramafic Unit|70276|5|Briefly described|p783-787, 790, 794|||Presented as [very informal] Mount Keith ultramafic unit. Mount Keith Domain, Yilgarn Craton. Over 500m thick. Proximal intrusive facies. Hosts disseminated Ni sulfides. Highly crust-contaminated. S isotope data tabulated.|2706 +/- 36 Ma.|||In contact with (probably intrudes) Mount Keith Dacite.|Numerous spinifex-free adcumulate-textured komatiite pods and lenses which are flanked by laterally extensive ortho- and mesocumulate-textured units. Contains widespread hydrous magmatic mineral phases.|
75824|Mount Keith Ultramafic Unit|70863|6|Mentioned|p12|||Yilgarn Craton.||||||
75824|Mount Keith Ultramafic Unit|71212|6|Mentioned|p256|||||||Laterally equivalent to the Agnew Komatiite.||
75824|Mount Keith Ultramafic Unit|73596|6|Mentioned|p1151, 1156|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt. Appears as Mt Keith Ultramafic Unit.|c.2715 Ma (maximum eruption age).|||Equivalent to Wiluna, Perseverance, Ultramafic Units.||
83878|Mount Keith ultramafic sequence|69414|6|Mentioned|p101|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton.|c.2709-2013 Ma (age of footwall).|||||
24402|Mount Leake Sandstone|7161|5|Briefly described|p90|Statherian|Statherian|Mount is spelt Mt in the text. Age determined using detrital zircons.|1774 +/- 20 Ma|||||02-MAY-12
24402|Mount Leake Sandstone|22493|6|Mentioned|p90|Statherian|Statherian|1774+/-20Ma,  Mount is written Mt in text||||||
24402|Mount Leake Sandstone|35975|2|Defined|p104|Proterozoic|Proterozoic|||||||
24402|Mount Leake Sandstone|37299|6|Mentioned|p88|||||||||
24402|Mount Leake Sandstone|38243|6|Mentioned|Fig.2|||||||||
24402|Mount Leake Sandstone|38994|6|Mentioned|p34|||||||||
24402|Mount Leake Sandstone|40297|6|Mentioned|Fig.1|||||||||
24402|Mount Leake Sandstone|40938|6|Mentioned|p5|||||||||
24402|Mount Leake Sandstone|40989|4|Described|p32|||||||||
24402|Mount Leake Sandstone|43069|1|Redefined|p31||Mesoproterozoic|refer to Gee (1979) for original definition.||||||
24402|Mount Leake Sandstone|65419|5|Briefly described|pp48-50.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979, 1987) and Elias et al. (1982); revised by Gee and Grey (1993); name changed to Mount Leake Formation and redefined in this study. A K-Ar age of 1573 Ma was obtained from glauconite in this unit, but is dubious since that is younger than the initial rifting of the overlying Bangemall Group at c.1.63-1.64 Ga (Nelson, 1995).||||||
41123|Mount Leonora chert|24196|6|Mentioned|p69 Fig. 10|||Mount is Mt. in text. Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||
37995|Mount Leopold Sandstone|23484|6|Mentioned|p27 Fig. 12|||Sandstone and basalt of the Mount Roe Basalt at the base of the Fortescue Group, near Mount Leopold.||||||11-MAY-15
38660|Mount Lucky conglomerate|23786|5|Briefly described|p27|||Informal name - see Mount Lucky Conglomerate.  Geological Province: Yilgarn Craton.||||||
38660|Mount Lucky conglomerate|62083|5|Briefly described|p1014 Fig.6, p1015 Fig.7|||Main gold camp: Laverton.|||||Conglomerate-arenite.|
38664|Mount Lucky granodiorite|23786|5|Briefly described|p34 Tb. 4|||Informal name.  Geological Province: Yilgarn Craton.||||||
75237|Mount MacLeod Member|44152|5|Briefly described|p179 Fig.2-155|||||Marra Mamba Iron Formation||Overlies Nammuldi Member. Is overlain by Mount Newman Member.|Shale.|
75237|Mount MacLeod Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Marra Mamba Iron Formation.||||||23-JUN-09
34352|Mount Manypeaks Pluton|22737|6|Mentioned|9|||||||||
31916|Mount Marquis Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite.||||||07-FEB-11
31916|Mount Marquis Granite|50425|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
35855|Mount McCrae Shale|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group. Misspelling of Mount McRae Shale.||||||
35855|Mount McCrae Shale|24544|5|Briefly described|p59|Paleoproterozoic|Archean|Probably Misspelt. See Mount McRae Shale. Geological Province: Hamersley Basin.||||||07-NOV-08
74143|Mount McDonald Granite|62107|6|Mentioned|p1391 Fig. 2|||Age: <2643+/-6Ma. Mount is Mt in text of figure.||||||
82073|Mount McGrath Beds|72712|6|Mentioned|p7, p31, p34.|||Of McLeod et al. (1963). Previously considered to be equivalent to the Nummana Member. Replaced by Mount McGrath Formation in 1964.||||||
75796|Mount Minnie Formation|24607|6|Mentioned|p969 Fig.2|||See also Mount Minnie Group. Unconfomable over Ashburton Formation in NW?||||||
36852|Mount Monger Sill|23582|5|Briefly described|Map Legend|Archean|Archean|Gabbro, relict cumulate texture; metamorphosed.||||||07-NOV-08
25289|Mount Narryer quartzite sequence|41942|6|Mentioned|p67|||||||||
28806|Mount Narryer sequence|41942|6|Mentioned|p67|||||||||
80618|Mount Negri Basalt|71803|6|Mentioned|p369|Mesoarchean|Mesoarchean|Western Pilbara Craton.|ca. 2950 Ma|||||12-NOV-18
70135|Mount Negri Volcanic Member|63441|5|Briefly described|p5 Tb.1|Archean|Archean|Of Bookingarra Formation (Croydon Group, De Grey Supergroup). Geological province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
70135|Mount Negri Volcanic Member|64174|5|Briefly described|Map legend|Archean|Archean|Of the Bookingarra Formation (Croydon Group, De Grey Supergroup).  Geological province: Mallina Basin. Basalt, komatiitic basalt and basaltic andesite; local siliciclastic sedimentary rocks; metamorphosed.||||||07-NOV-08
70135|Mount Negri Volcanic Member|64580|4|Described|map legend||Mesoarchean|Of Bookingarra Formation. Basalt, komatiitic basalt and basaltic andesite;local siliciclastic sedimentary rocks; metamorphosed.||||||15-DEC-08
70135|Mount Negri Volcanic Member|64632|6|Mentioned|p203|Mesoarchean|Mesoarchean|Compared with basalts on northern (Salt Well Member & NE (Coonieena Basalt Member) margins of East Pilbara Terrane||Of the Bookingarra Formation|||Spinifex and variolitic textured basalts.|
70135|Mount Negri Volcanic Member|67201|4|Described|p21 Fig.12, p23-24, p58-59, p63|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin. "Negro Volcanics" mentioned on p24 in previous interpretations section, where "Negri" is misspelt as "Negro". Shortened to Mount Negri Volcanics on some figures.||Bookingarra Formation||Louden Volcanic and Mount Negri Volcanic Members overlie (and overlap with) Rushall Slate in Whim Creek greenstone belt.|Siliceous high-Mg basalt. Variolitic and characterised by only fine spinifex-texture.|24-NOV-16
70135|Mount Negri Volcanic Member|69185|4|Described|500k_geologyp08_lut.csv||Mesoarchean|Geological Province: Pilbara Craton.||Unit of Bookingarra Formation.|||Basalt, komatiitic basalt and basaltic andesite; local siliciclastic sedimentary rocks; metamorphosed|
70135|Mount Negri Volcanic Member|69301|5|Briefly described|p15|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Mallina Basin.||Bookingarra Formation|||Siliceous high-Mg basalt.|
70135|Mount Negri Volcanic Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt|
70135|Mount Negri Volcanic Member|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.||Bookingarra Formation|||Basalt, komatiitic basalt, and basaltic andesite; local siliciclastic sedimentary rocks; metamorphosed.|
70135|Mount Negri Volcanic Member|72668|6|Mentioned|p14-15|||Spelt Negri Volcanic Member p15. Basalts similar to this occur across the Mallina Basin.||Bookingarra Formation.||Overlies the Cistern Formation.|Locally spinifex-textured and variolitic basalts.|13-JAN-22
79181|Mount Newman Formation|65757|5|Briefly described|p84 Fig.2||Neoarchean|underlies the Bee Gorge Member, [misspelling of Mount Newman Member] shown as part of the Marra Mamba Iron Formation.||||||
41462|Mount Nulasy Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
41462|Mount Nulasy Granite|50437|5|Briefly described|p1.6, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1856 +/- 10Ma (Shrimp).||||||07-NOV-08
81399|Mount Palgrave Group, Lower|67553|4|Described|p40-41|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Typically contains more local unconformities and higher proportion of high-energy deposits (breccia, conglomerate etc) in the vicinity of Barrow Range anticline. Basal rhyolite units in proximity to, or contact with Winburn Granite have a slightly coarser, crystalline appearance due to the thermal overprint. Shown as 'lower Mount Palgrave Group' in text p45, 94.||||Underlain and intruded by Winburn Granite.|Rhyolites and ignimbrites, flow banded feldspar-phyric flows. Stratified pyroclastic rocks, autoclastic breccia, with intercalated basalt, andesite and siliciclastics rich in volcanogenic detritus. Upper section of coarse clastic diamictite.|16-AUG-19
81396|Mount Palgrave Group, Upper|67553|5|Briefly described|p40-41|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Eutaxitic (i.e. these are rheomorphic ignimbrites), rather than indicating an origin as a primary volcanic (effusive) flow. Shown as informal 'upper Mount Palgrave Group' p46, 47, 95, 97.|||||Massive to flow-banded, feldspar(-quartz)-phyric rhyolite, and lesser trachyte and dacite with locally significant intercalations of crystal-rich ignimbrite and siliciclastic rocks (interbeds of microbial laminites).|16-AUG-19
69028|Mount Pickering dolerite|60978|6|Mentioned|p68-69 Fig.3|||Informal reference to a dolerite in the Darlot gold deposit area. Informal - see Mount Pickering Dolerite. Geological Province: Yilgarn Craton.||||||25-MAY-05
69028|Mount Pickering dolerite|60981|4|Described|p178, p177 Fig.2, p201|||Informal name. Also referred to as the Mount Pickering dolerite sill. See also p182 Table 2, p183 Fig.5. Geological Province: Yilgarn Craton. Max. thickness: ~600m.||||||
78644|Mount Pleasant Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 5 unnamed subunits.||Massive olivine cumulate (dunite) at base; pyroxenite; gabbro; leucogabbro and plagioclase-rich gabbronorite; gabbronorite marker horizon; all metamorphosed.|06-AUG-15
78644|Mount Pleasant Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Dunite, pyroxenite, gabbro, leucogabbro and gabbronorite; metamorphosed.|
78644|Mount Pleasant Intrusion|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 100k_geologyl10_lut.csv.|||||Massive olivine cumulate (dunite) at base; metamorphosed; gabbro, leucogabbro, gabbronorite, plagioclase-rich gabbronorite; metamorphosed; pyroxenite.|
69029|Mount Pleasant dolerite|60978|6|Mentioned|p68-69 Fig.3|||Informal reference to a dolerite in the Kalgoorlie region. Geological Province: Yilgarn Craton.||||||
34529|Mount Ragged Metasediments|22792|6|Mentioned|p56|||||||||
34529|Mount Ragged Metasediments|67722|5|Briefly described|p1, p12, p19-20|||Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen. Also referred to as Mount Ragged Formation, p5. Metamorphosed at 1154+/-15 Ma. |||||Massive quartzites and subordinate upper greenschist to lower amphibolite facies metapelites.|
80504|Mount Ragged Quartzite|63866|4|Described|p191|Ectasian|Ectasian|Deposited in deep water conditions. Detrital zircons at c. 1780 Ma and c. 1320 Ma are consistent with derivation from the Dalyup Gneiss and Recherche Granite.|1321 +/- 24 Ma (Maximum depositional age)||||Quartzite and minor pelite.|
31152|Mount Ragged Schist|43498|5|Briefly described|6|||||||||
31152|Mount Ragged Schist|69252|6|Mentioned|p22|||Myers (1995). Subsequently the Mount Ragged Formation (Spaggiari et al., 2009).||||||
68062|Mount Ragged metasedimentary rocks|24526|5|Briefly described|p106 Fig. 7, p108|Mesoproterozoic|Mesoproterozoic|Informal term repeatedly used to describe rocks within the Nornalup Complex.  Sequence of quartzite and minor pelite.  Unconformably overlies the Recherche Granite. See also p105 Fig. 6 (MRM).||||||02-MAR-05
68062|Mount Ragged metasedimentary rocks|64722|5|Briefly described|Fig. 2 p. 3-6, p19, 28|Ectasian|Ectasian|Informal. Of the Albany-Fraser Orogen.||||Unconformable on the Recherche Granite.||11-APR-12
80503|Mount Ragged schist|63866|5|Briefly described|p191|||Described along with the 'Mount Ragged metasedimentary rocks' as: a sequence of massive quartzites and subordinate metapelites recrystallised in upper greenschist-lower amphibolite facies.|||||Massive quartzites and subordinate metapelites.|29-MAR-18
35849|Mount Ramsay dolerite|23328|6|Mentioned|1030, 1031|||||||||07-SEP-09
35849|Mount Ramsay dolerite|65337|6|Mentioned|p94.|||Shown in inverted commas to emphasise informal status.||Unit in Kalkarindji Volcanic Group.||||
35849|Mount Ramsay dolerite|69445|5|Briefly described|p30:1, 10, 16-17|||Glass (2002). Kimberley region. Informal name. Interpreted as a feeder dyke for the Antrim Plateau Volcanics/Kalkarindji Suite.||Kalkarindji Suite.||||12-JUL-16
73867|Mount Roe Group|24550|6|Mentioned|p32|||Geological Province: Hamersley Basin. Mount is Mt in text.||||||07-FEB-11
78674|Mount Roe Sequence|60112|5|Briefly described|p108-109 Fig.2, p111-112, p117. ||||ca. 2772 Ma (Arndt et al., 1991; Wingate, 1999)|Basal unit in Fortescue Group.||Unconformably to disconformably overlain by the Glen Herring Creek Sequence.|Includes basal sediment beneath ~2.5 km of subaerial tholeiitic basalt.|
39729|Mount Roe flood basalts|24192|6|Mentioned|p870|||Informal name - see Mount Roe Basalt.  Of the Fortescue Group. Geological Province: Pilbara Craton.||||||31-JAN-08
39731|Mount Scholl gabbro|24192|6|Mentioned|p853, Fig.3|Archean|Archean|Geological Province: Pilbara Craton. Not intended as a formal name||||||07-NOV-08
34314|Mount Scholl intrusion|22676|6|Mentioned|p284|||Pilbara Block||||||
72449|Mount Shea porphyry|62107|6|Mentioned|p1391 Fig. 2|||Informal name. In the Eastern Goldfields Province.||||||
72449|Mount Shea porphyry|66880|6|Mentioned|p11. |Archean|Archean||2658 +/- 3 Ma (Krapez et al. 2000).|||Intrudes the Kalgoorlie Sequence.||
76798|Mount Silvia Formation|64725|6|Mentioned|p58.|||||Unit in Hamersley Group.||Overlies Wittenoom Dolomite. Is overlain by Mount McRae Shale.||
73908|Mount Sylvia Shale Formation|50227|5|Briefly described|p443 Fig. 1|||Conformably overlain by Dales Gorge Member.||||||07-FEB-11
28814|Mount Sylvia shale|37591|6|Mentioned|p32|||||||||
75275|Mount Thirsty Intrusion|65264|5|Briefly described|p23, p49 Appdx. 1|Archean|Archean|Comprises lower cumulate-textured pyroxenite, locally underlain by serpentinitised peridote and overlain by upper units of norite and gabbro, and quartz gabbro with granophyric segregations. More lithological details on p49 Appdx. 1.||||||07-FEB-11
75275|Mount Thirsty Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 3 unnamed subunits.||Pyroxenite; includes dunite and olivine bronzitite layers and minor peridotite; quartz gabbroic and granophyric segregations in gabbro; gabbro; minor granophyric and quartz gabbro; all metamorphosed.|06-AUG-15
75275|Mount Thirsty Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Pyroxenite: includes dunite and olivine bronzitite layers and minor peridotite; quartz gabbroic and granophyric segregations in gabbro; gabbro: minor granophyric and quartz gabbro. All metamorphosed.|
75275|Mount Thirsty Intrusion|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 100k_geologyl10_lut.csv.|||||Gabbro, and quartz gabbroic and granophyric segregations in gabbro; metamorphosed; Pyroxenite; includes dunite and olivine bronzitite layers and minor peridotite; metamorphosed.|
25296|Mount Vernon Sandstone|22905|6|Mentioned|p52 Fig. 2, p54|Mesoproterozoic|Mesoproterozoic|Superseded by Calyie Formation (Collier Group).  Mount as Mt. in text.||||||24-JAN-06
25296|Mount Vernon Sandstone|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Kurabuka Formation. U'lying unit Fords Creek Shale. Geological Province: Bangemall Basin. Max. thickness: 240 m.||||||
25296|Mount Vernon Sandstone|24183|5|Briefly described|p4 Fig.3|Mesoproterozoic|Mesoproterozoic|Mount is spelt Mt. in text. Of the Dooley Subgroup (Chuck 1984). Equivalent of the Calyie Formation.||||||
25296|Mount Vernon Sandstone|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Superseded by Calyie Formation. Overlies Fords Creek Shale. Overlian by Kurabuka Formation. Of Dooley Subgroup. Mount written Mt in text.||||||01-FEB-05
25296|Mount Vernon Sandstone|29916|4|Described|p118|||||||||
25296|Mount Vernon Sandstone|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25296|Mount Vernon Sandstone|36551|6|Mentioned|p101|||||||||
25296|Mount Vernon Sandstone|37460|4|Described|Table 3.VI|||||||||
25296|Mount Vernon Sandstone|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25296|Mount Vernon Sandstone|38299|4|Described|p11|||||||||
25296|Mount Vernon Sandstone|40089|2|Defined|p38|Mesoproterozoic|Mesoproterozoic|||||||
25296|Mount Vernon Sandstone|40899|6|Mentioned|Fig.1|||||||||
25296|Mount Vernon Sandstone|41360|6|Mentioned|p192|||||||||
25296|Mount Vernon Sandstone|42471|4|Described|p21|||||||||
25296|Mount Vernon Sandstone|42472|5|Briefly described|Map legend|||||||||
25296|Mount Vernon Sandstone|44142|4|Described|p312 Tb.4-4, p319-320, p322|||~225m thick. Originally (Daniels, 1969) mapped as base of Kurabuka Formation. Within Dooley Subgroup of Chuck (1984). Deposited on shoreline barrier-bar or tide-swept shelf with bipolar current directions (east-west).||Mucalana Subgroup.||Overlies and interfingers with Fords Creek Shale conformably. Direct correlate of Calyie Sandstone. Overlain by Kurabuka Formation conformably. Interfingers with Fords Creek Shale.|Fine- to medium-grained arenite; rare conglomerate; local interbedded siltstone, shale and glauconitic sandstone.|13-MAR-18
25296|Mount Vernon Sandstone|50225|5|Briefly described|p387 Fig. 2|||Superseded by Calyie Formation (Edmund Group).  Mount is Mt. in text.  Of the former Mucalana and Dooley Subgroups (Bangemall Group).||||||07-FEB-11
25296|Mount Vernon Sandstone|63869|6|Mentioned|p41|||Muhling and Brakel,(1985). Obsolete: of the superseded Mucalana Subgroup. Replaced by Calyie Sandstone (Cooper et al., 1998), later renamed Calyie Formation (Martin et al., 1999) to reflect its lithological variation.||||||
77232|Mount Waugh rhyolite|67375|5|Briefly described|p46.|||An informal name for a unit at the faulted southern edge of the Scamp area.|||||Flow-banded, sparsely quartz- and feldspar-phyric rhyolite.|
77232|Mount Waugh rhyolite|67553|5|Briefly described|p46,48,50|||Geological province: Musgrave Province, North Australian Craton. Informal term for a rhyolitic unit that forms a prominent exposure at the Mount Waugh area (<1km north of Kathleen Ignimbrite on MOUNT EVELINE 1:100 000 map sheet). Includes alteration regions where the original rhyolitic assemblage is transformed to a schistose quartz- and muscovite-rich assemblage (locally contains veins, stringers, and nodular, granoblastic, aluminosilicate minerals, including kyanite and andalusite).|||||Flow banded, sparsely quartz- and feldspar-phyric rhyolite.|
77232|Mount Waugh rhyolite|68995|5|Briefly described|p7 Fig.3, p13-15, p18, p21, p27 Tb.2|||Talbot Sub-basin. Informal name. Petrology discussed in detail. See also p29, p35 Fig.20, p43, p45-46.||Mount Palgrave Group||Overlies the Scamp Formation and the Eliza Formation. Overlain by the Kathleen Ignimbrite.|Flow-banded, poorly sorted, sparsely quartz- and feldspar-phyric rhyolites and silica-rich rhyolites.|
77232|Mount Waugh rhyolite|69091|6|Mentioned|p71 Fig.4.14|||informal||Mount Palgrave Group||||
77232|Mount Waugh rhyolite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Mount Palgrave Group.||||
77232|Mount Waugh rhyolite|70095|5|Briefly described|p16-17,19|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Also referred to as Mount Waugh Formation on p19. Thickness of rhyolitic package: 1.5km, and over 75km strike length, estimated in volume to be over 3375km3. See p19 Table 2 for U-Pb zircon data.||Unit of Mount Palgrave Group.||Uppermost unit of Mount Palgrave Group. Overlain by Kaarnka Group/Pussy Cat Group. Underlain by Scamp Formation.||
80613|Mount Webber Suite|72251|6|Mentioned|p54|Paleoarchean|Paleoarchean|Note that Mount Webber Gabbro is used in the rest of the paper.||||||
80613|Mount Webber Suite|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||||||
23839|Mount Weld carbonatite|23573|6|Mentioned|p3|||Informal - see Mount Weld Carbonatite||||||
23839|Mount Weld carbonatite|24168|6|Mentioned|p646|||Mount is Mt in text.  Informal name.||||||
23839|Mount Weld carbonatite|24494|5|Briefly described|p31|Paleoproterozoic|Paleoproterozoic|Age: 2021 +/- 13 Ma. See also Mount Weld Carbonatite||||||07-NOV-08
23839|Mount Weld carbonatite|37460|5|Briefly described|p188|||||||||
23839|Mount Weld carbonatite|40170|6|Mentioned|p159|||||||||
23839|Mount Weld carbonatite|40811|4|Described|p315|||||||||
23839|Mount Weld carbonatite|41255|5|Briefly described|p67|||||||||
23839|Mount Weld carbonatite|41262|5|Briefly described|p38|||||||||
23839|Mount Weld carbonatite|62083|5|Briefly described|p1015 Fig.7|Proterozoic|Proterozoic|Main gold camp: Laverton.|||||Granitic intrusion.|
23839|Mount Weld carbonatite|64329|6|Mentioned|p27 Tb. 7|||Presented as a selected thorium deposit. Production of rare earths anticipated in late 2008.||||||29-JUL-08
23839|Mount Weld carbonatite|65343|5|Briefly described|p12|||Lottermoser (1990) used REE data from the deeply weathered Mount Weld carbonatite near Laverton (WA) to demonstrate REE are mobilised and fractionated during regolith development, in contrast to the relatively low REE and Y contents in the unweathered Mount Weld carbonatite. Includes lateritic REE phosphate deposits.||||||
23839|Mount Weld carbonatite|70271|6|Mentioned|p541|||Laverton area, Eastern Goldfields province, Yilgarn Craton. A K-Ar age of 2064 +/- 40 Ma is also given.|2021 +/- 13 Ma; Rb-Sr (Duncan and Willett, 1990).|||||
23839|Mount Weld carbonatite|70292|6|Mentioned|p339|Rhyacian|Rhyacian|Located 15 km ESE of Granny Smith. Related to lamprophyre dykes. Written as Mt Weld carbonatite. See also Mt Weld intrusive suite p341, Mt Weld complex p358, Mt Weld Suite p341 Fig.2.|2100 Ma|||||
23839|Mount Weld carbonatite|71410|5|Briefly described|p1046, p1048, p1050|||REE-enriched rocks have a REE concentration in the regolith. Weathering processes discussed.||||||
34567|Mount Weld carbonatite complex|22814|5|Briefly described|p258|||Spelt "Mt" in text.  Overlying regolith a source of rare earths, tantalum-niobium and phosphate.||||||
28818|Mount Weld carbonatite laterite|41255|6|Mentioned|p67|||||||||
84051|Mount Weld intrusive suite|70292|5|Briefly described|p341|Rhyacian|Rhyacian|Considered to include east-west trending dikes of ultramafic lamprophyre and carbonatite up to 2 m thick (Ojala, 1995). Written as Mt Weld intrusive suite. Shown as Mt Weld suite p341, Fig.2. Mt Weld complex also used p358. See also Monut Weld carbonatite p339.|2100 Ma||||Includes calcite-cemented jig-saw breccia and olivine lamprophyre intrusive breccia.|
39223|Mount West metapelite|23892|6|Mentioned|p46|||Informal name. Mount is Mt. in text.||||||
79182|Mount Whaleback Member|65757|5|Briefly described|p84 Fig.2|||Banded iron formation, underlies the Joffre Member, overlies the Dales Gorge Member, part of the Brockman Iron Formation.||||||
76206|Mount Whaleback Shale|67056|6|Mentioned|p419 Fig.2. |||||Unit in Brockman Iron Formation.||Overlies Dales Gorge Member. Is overlain by Joffre Member.||
83716|Mount White Formation|70275|5|Briefly described|p471|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.||||Overlies Vivien Sedimentary Formation. Is overlain by Jones Creek Conglomerate.|Basalt.|
83716|Mount White Formation|70276|6|Mentioned|p784|||||||||
82962|Mount White Sequence|73238|6|Mentioned|p13 Fig.10|||||||||
73562|Mowanjum formation|36483|5|Briefly described|p74|||Name used informally - see Mowanjum Sand.||||||
32737|Mowla Formation|7433|6|Mentioned|p45 Fig.35.|||Mis-named for Mowla Sandstone (see also p25 Fig.2, p42, p44).||||||
32737|Mowla Formation|44998|14|Not recorded|p.119|||||||||
83555|Moyle Formation|73083|6|Mentioned|p16|Mesoproterozoic|Mesoproterozoic|[Probably a misspelling of Moyle River Formation].||||||
29778|Mr McGrath Formation|43037|5|Briefly described|Table 1,p24|||misspelling of Mount McGrath Formation||||||
27849|Mt McRae Shale|29716|4|Described|Table 1|||||||||
27849|Mt McRae Shale|71513|6|Mentioned|p66-67, p70, p74, p85, p87-88|||Pilbara Craton. Interpreted to have been deposited on a continental shelf.||Hamersley Group|Includes the Colonial Chert Member.|Overlies the Marra Mamba Iron Formation. Overlain by the Brockman Iron Formation and the Boolgeeda Iron Formation.|Organic-rich shales.|
23842|Mucalana Subgroup|22905|5|Briefly described|p52 Fig. 2, p54|Mesoproterozoic|Mesoproterozoic|Replaced by Collier Group.  Previously comprised Kurabuka Formation, Mount Vernon Sandstone and Fords Creek Shale.||||||24-JAN-06
23842|Mucalana Subgroup|24115|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of the Collier Group. Geological Province: Collier Basin.||||||
23842|Mucalana Subgroup|24183|5|Briefly described|p3 Fig.2, p4 Fig.3, p21|Mesoproterozoic|Mesoproterozoic|Abandoned name - now obsolete - constituent formations renamed and incorporated into the Collier Subgroup (Cooper et al, 1998b). Geological Province: Bangemall Basin. Of the Collier Group.||||||
23842|Mucalana Subgroup|24535|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Rocks now incorporated into the Collier Group. Geological Province: Collier Basin.||||||26-NOV-13
23842|Mucalana Subgroup|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Superseded by Collier Group. Overlies Edmund Subgroup.||||||
23842|Mucalana Subgroup|40089|2|Defined|p36|Mesoproterozoic|Mesoproterozoic|||||||
23842|Mucalana Subgroup|42471|5|Briefly described|p21, p19|||||||||
23842|Mucalana Subgroup|44142|5|Briefly described|p309 Fig.4-13, p310 Tb.4-3, p311|||See also p312 Tb.4-4, p319-320, p322. Regressive linear-shoreline sequence. Now interpreted as a western extension of the Collier Subgroup over the older Edmund Subgroup.||Bangemall Group|Fords Creek Shale, Mount Vernon Sandstone, Kurabuka Formation.|Conformably overlies Edmund Subgroup.||
23842|Mucalana Subgroup|50225|5|Briefly described|p387 Fig. 2|||Of Muhling and Brakel (1985).  Formerly of the Bangemall Group - became part of the Dooley Subgroup (Bangemall Group) - superseded by Collier Group.||||||07-FEB-11
23842|Mucalana Subgroup|63869|6|Mentioned|p28, p39, p40, p41|||Of Muhling and Brakel (1985). Obsolete (Cooper et al., 1998); rocks now included in Collier Group which was elevated from Subgroup status by Martin et al. (1999).||||||
39764|Mucca granitoid complex|24193|5|Briefly described|p874 Fig.1, p878 Tb.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
72902|Muccan Granitic Complex|62576|6|Mentioned|p619|||||||||
72902|Muccan Granitic Complex|63441|5|Briefly described|p26|Archean|Archean|Lithostructural term for metagranitic rocks unconformably overlain by the former Nimingarra Iron Formation rocks which are now assigned to Cleaverville Formation. Age: c.3.44Ga. Geological province: Pilbara Craton.||||||07-FEB-11
72902|Muccan Granitic Complex|64580|4|Described|map legend||Neoarchean|Undivided granitoid rock; metamorphosed.||||||15-DEC-08
72902|Muccan Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
72902|Muccan Granitic Complex|65827|6|Mentioned|p15, p16|Paleoarchean||Granitic components contain inherited 3650-3550 Ma zircons indicative of ancient sialic crust; has a central c.3240 Ma intrusion.
||||||
72902|Muccan Granitic Complex|66217|4|Described|p1, p2, p6 Table 1, p11, p12, p24, p32. |||Components of this Complex have five main age groupings: c.3470, 3420, 3310, 3250 and 2940 Ma. Outcrops as subdued, undulating topography. Separated from the Carlindi Granitoid Complex to the west by the Warralong greenstone belt of Pilbara Supergroup rocks. Includes pods and linear units of metaperidotite and metapyroxenite.|c.3470 to 2940 Ma.||Includes Tambina, Callina, Emu Pool and Cleland Supersuites.|Intrudes Warrawoona Group. Is intruded by Black Range Dolerite Suite. Is unconformably overlain by De Grey Supergroup.||
72902|Muccan Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
72902|Muccan Granitic Complex|70022|6|Mentioned|p113-114, 116|||East Pilbara Terrane.||Cleland Supersuite.|Wolline Monzogranite.|Adjacent to the Warrawagine Granitic Complex.||
36886|Muccan Granitoid Complex|23415|5|Briefly described|Map Legend|Archean|Archean|Geological province: Pilbara Craton. Metamorphosed, fine- to coarse-grained monzogranite, syenogranite, granodiorite, and tonalite; massive seriate and porphyritic varieties; foliated to gneissic; minor banded gneiss.||||||07-NOV-08
36886|Muccan Granitoid Complex|23585|6|Mentioned|p12|Archean|Archean|||||||07-NOV-08
36886|Muccan Granitoid Complex|23757|4|Described|p5, p10|Archean|Archean|Unconformably overlain by Gorge Creek and De Grey Groups.  Age: c.3470-3240 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
36886|Muccan Granitoid Complex|23783|5|Briefly described|p84|Archean|Archean|||||||07-NOV-08
36886|Muccan Granitoid Complex|23807|5|Briefly described|p111|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36886|Muccan Granitoid Complex|23895|5|Briefly described|p884 Fig.1, p904|||Geological Province: Pilbara Craton.||||||07-MAR-05
36886|Muccan Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3470-3244Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36886|Muccan Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
36886|Muccan Granitoid Complex|24590|5|Briefly described|p40|Archean|Archean|Granites. Age: 3.25-3.20Ga. Geological Province: Marble Bar Domain.||||||07-FEB-11
36886|Muccan Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p146 Tb.2-21, p152|||See also p153 Fig.2-140, p155 Fig.2-142. No named constituents.|||||Porphyritic monzogranite, foliated granodiorite, monzogranite, gneiss and migmatite, greenstone (mafic schist).|
36886|Muccan Granitoid Complex|44229|5|Briefly described|Map legend|Archean|Archean|Contains the Wolline Monzogranite.  Metamorphosed fine- to coarse-grained monzogranite, syenogranite, granodiorite, and tonalite.||||||07-NOV-08
36886|Muccan Granitoid Complex|50189|4|Described|p15-16|Archean|Archean|Contains the Wolline Monzogranite intrusive stock. Unconfomably overlain by Gorge Creek Group. Age: c.3470Ma, c.3244Ma; also 3313Ma (Nelson, 1998), c.3300 and c.3440Ma.||||||07-NOV-08
36886|Muccan Granitoid Complex|50383|5|Briefly described|Map Legend|Archean|Archean|Includes the Wolline Monzogranite.  Geological Province: Pilbara Craton||||||07-NOV-08
36886|Muccan Granitoid Complex|50427|6|Mentioned|p182 Fig.5|Archean|Archean|||||||07-NOV-08
36886|Muccan Granitoid Complex|50544|3|Fully described|p28-29, p10 Fig. 5|Archean|Archean|Xenolith-rich, strongly foliated, gneissic granitoid and gneiss.  Unconformably overlain by Gorge Creek Group in the north-east.  Age: c.3470-3244Ma (Nelson, 1996, 1998; Williams, 1999a).||||||23-DEC-09
36886|Muccan Granitoid Complex|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Wolline Monzogranite.  Age: 3470-3244Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36886|Muccan Granitoid Complex|60429|4|Described|p6 Fig. 3, p15-16|Archean|Archean|Unconformably overlain in parts by Gorge Creek Gp. Overlying Nimingarra Iron Fm. forms the NE boundary of the complex. Age:c.3438Ma; also obtained: c.3470Ma, c. 3244Ma. Geol.prov: Pilbara Craton. Detailed lithology is presented. See also p8 Fig. 4.||||||07-FEB-11
36886|Muccan Granitoid Complex|60636|6|Mentioned|p11|||||||||07-FEB-11
36886|Muccan Granitoid Complex|62427|6|Mentioned|p4|||N of Coppin Gap Greenstone Belt.||||||
36886|Muccan Granitoid Complex|64326|6|Mentioned|p71 Fig. 1|Archean|Archean|Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
36886|Muccan Granitoid Complex|64936|5|Briefly described|map legend|Archean|Archean|Includes Wolline Monzogranite. Monzogranite, granodiorite, and tonalite; metamorphosed. Age range: c. 3250 - c. 3470 Ma (geochron). Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||
36886|Muccan Granitoid Complex|69167|6|Mentioned|178022.1.pdf|Archaean|Archaean|(Structural?)Age derived from sample of porphyritic biotite tonalite (178023.1.pdf)|3420 +/-3 Ma (SHRIMP)|||||
42415|Muccan granitoid complex|24590|6|Mentioned|p132 Fig. 4.2|||Informal - see Muccan Granitoid Complex.||||||07-FEB-11
42415|Muccan granitoid complex|50189|6|Mentioned|p22|||Informal - see Muccan granitoid complex. Age: c.3313Ma.||||||
42402|Muderup Beach Rock|23816|6|Mentioned|p256|Quaternary|Quaternary|Geological Province: Perth Basin.||||||16-DEC-04
27509|Mudjalla Sandstone "Member"|36224|5|Briefly described|Map legend|Early Jurassic|Early Jurassic|Sandstone, medium to coarse, poorly sorted, cross-bedded; siltstone, very fine sandstone, planar-bedded, ripple marked.Early? to Late Jurassic.||||||01-FEB-05
79287|Mugga Murra Dolerite Suite|70226|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province. Shown as Mugga Murra Suite on Interpreted Bedrock Geology figure.|c. 1210 Ma.|Marnda Moorn Supersuite|||Dolerite and gabbro dykes. Diorite to leucogabbronorite dykes, up to 40 m wide and locally with orthopyroxene cumulate crystals up to 7 mm; locally microdiorite.|16-DEC-15
79236|Muggamurra Dolerite Suite|69583|5|Briefly described|Plate 3|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province. See also Muggamurra Suite (p58, p82; Plate 2).|c.1210 Ma.|Marnda Moorn Supersuite.|||Dolerite and gabbro dykes.|
79236|Muggamurra Dolerite Suite|70140|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Marnda Moorn Large Igneous Province. Also appears as MuggaMurra Dolerite Suite.||Marnda Moorn Supersuite.|||Dolerite and gabbro dykes.|
79236|Muggamurra Dolerite Suite|70795|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic||1215-1205 Ma||||Dolerite and gabbro.|
79236|Muggamurra Dolerite Suite|70796|5|Briefly described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Part of the Marnda Moorn Large Igneous Province. Mapping code is: P_MMUod. Also appears as Muggamurra Dyke Suite in file:  2_5m_interpdykel15_lut.csv. See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 185931.1.pdf, Yalgoo100_2241_stratig.pdf, Youanmi100_2640_stratig.pdf. Appears as Mugga Murra Dolerite Suite in Yalgoo100_2241_stratig.pdf (misspelling).|ca 1215 to 1205 Ma (inferred)|Marnda Moorn Supersuite|||Dolerite and gabbro dykes; diorite and leucogabbronorite dykes.|
79236|Muggamurra Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Ectasian|Ectasian|North Yilgarn Craton.|1215-1205 Ma|||||
79236|Muggamurra Dolerite Suite|71269|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Of Marnda Moorn Large igneous Province. Events: Warakurna Supersuite Magmatic Event (1084-1040 Ma); Marnda Moorn Supersuite Magmatic Event (1218-1202 Ma). Includes numerous dolerite and diorite dykes in the Murchison region that trend ENE to ESE. Sample GSWA 185931 (qtz diorite dyke) yielded a weighted mean 207Pb/206Pb date of 1210+\-11 Ma, interpreted as the magmatic crystallization age of the quartz diorite dyke. See 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1215-1205 Ma (inferred)|Unit of Marnda Moorn Supersuite.|||Dolerite and gabbro dykes|
79236|Muggamurra Dolerite Suite|71270|4|Described|2_5m_interpdykel15_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Yilgarn Craton, West Australian Craton. Events: Warakurna Supersuite Magmatic Event (1084 - 1040 Ma); Marnda Moorn Supersuite Magmatic Event (1218 - 1202 Ma).|1215-1205 Ma|Unit of Marnda Moorn Supersuite.|||Dolerite and gabbro dykes|
79236|Muggamurra Dolerite Suite|71271|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Marnda Moorn Large Igneous Province.|1215-1205 Ma.|Marnda Moorn Supersuite.|||Dolerite and gabbro dykes.|
79543|Muggamurra Dolerites|69003|6|Mentioned|p4|||Capricorn Orogen.||||||
80611|Muggamurra Dyke Suite|70830|5|Briefly described|p22|Stenian|Ectasian|Yilgarn Craton. Age is derived from a quartz diorite in the central Youanmi Terrane. shown as Mugamurra Suite in Fig. 19.|1210 +/- 11 Ma (Wingate and Kirkland, 2011)||||Dolerite, gabbro and diorite dykes.|12-NOV-18
75380|Muggamurra Suite|68561|5|Briefly described|GEOCHRON files|Mesoproterozoic|Mesoproterozoic|Murchison Domain, Youanmi Terrane. Altered quartz diorite dyke U-Pb zircon Age: 1210 +/- 11 Ma interpreted as the magmatic crystallization age. See geochron file 185931.1.pdf||Marnda Moorn Supersuite||||05-NOV-15
75380|Muggamurra Suite|69583|5|Briefly described|p58, p82; Plate 2|Proterozoic|Proterozoic|Northern Yilgarn Craton. Is also referred to, in the one short paragraph, as the Muggamurra Dyke Suite (and on p84-85), Muggamurra dyke swarm and Muggamurra swarm. See also Muggamurra Dolerite Suite (Plate 3).|c.1210 Ma.|Marnda Moorn Supersuite.|||Dolerite, gabbro and diorite dykes.|
75592|Muiron Member (OFF)|61555|5|Briefly described|p240, 243|Berriasian|Tithonian|Exmouth Sub-basin. Age based on palynology, dinoflagellates: in P. iehiense 4ciia-4cic subzones of Helby. Top of unit is maximum flooding surface.||Of Barrow Group.||Overlies Macedon Member.|Silty mudstone, siltstone, silty glauconitic argillaceous sandstone.|20-MAR-12
70221|Mukinbudin pegmatite|24410|6|Mentioned|p169 Tables 72, 73 and 74|||Informal name. ||||||
34417|Mulcana subgroup|22716|6|Mentioned|table4, p237|Ectasian|Ectasian|Age: 1300 Ma. Part of the Bangemall Basin succession.||||||
33904|Mulgadinnah Hill leucoadamellite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2943 Ma||||||07-NOV-08
41217|Mulgarra formation|50223|6|Mentioned|p346|||Misspelt and informal - see Mulgarra Sandstone.||||||
83122|Mulgathing Metamorphic Complex|72488|5|Briefly described|p4|||Forms part of the basement to the Olympic Dam District.|2.5 Ga.|||Is intruded by the Hiltaba Suite. Is overlain unconformably by the Gawler Range Volcanics.||
69630|Mullaloo Sandstone|61155|5|Briefly described|p15|Early Eocene|Late Paleocene|Age: 58-56Ma. Overlies and interfingers with Kings Park Formation. Geological Province: Perth Basin.||||||
69630|Mullaloo Sandstone|68254|6|Mentioned|p1036 Fig.2|Paleogene|Paleogene|See Mullaloo Sandstone Member in this paper.||||||20-JUL-15
31102|Mulliberry Granitoid Complex|43478|2|Defined|p29-34|||||||||
41124|Mulliberry granitoid complex|24196|6|Mentioned|p70|||Geological Province: West Malcolm sub-domain, Yilgarn Craton.||||||
40172|Mullingara Complex|24410|5|Briefly described|p141 Fig. 82|||Geological Province: Perth Basin.||||||
40172|Mullingara Complex|24595|6|Mentioned|p586 Fig. 1a|||Geological Province: Pinjara Orogen.||||||
35305|Mullingara Gneiss|23172|4|Described|Map Legend|Proterozoic|Proterozoic|||||||
34432|Mullingarra Complex|22716|5|Briefly described|table4, p238|Stenian|Stenian|||||||
34432|Mullingarra Complex|22786|6|Mentioned|p30|||||||||
34432|Mullingarra Complex|23174|6|Mentioned|p9||Proterozoic|||||||
34432|Mullingarra Complex|23279|5|Briefly described|p10|||||||||
34432|Mullingarra Complex|23788|5|Briefly described|p5|||||||||
34432|Mullingarra Complex|24115|5|Briefly described|p29 Fig.27|Mesoproterozoic|Mesoproterozoic|Metamorphism c. 1060 Ma. Geological Province: Pinjarra Orogen.||||||
34432|Mullingarra Complex|24160|6|Mentioned|p23|||||||||
34432|Mullingarra Complex|24526|5|Briefly described|p106 Fig. 7, p113|Proterozoic|Proterozoic|Dominated by psammitic paragneiss with conformable lenses of pelite, quartzite and mafic gneiss.  Unconformably overlain by the Yandanooka Group.   Geol.Prov: Carnarvon Basin. See also Mullingarra gneiss and Mullingarra paragneiss.  See also p112 Fig. 9.||||||14-JUN-05
34432|Mullingarra Complex|24535|6|Mentioned| p19 Fig.15|||Metamorphism ~1060 Ma.||||||26-NOV-13
34432|Mullingarra Complex|24542|5|Briefly described|p2 Fig.2, p4|Proterozoic|Proterozoic|Psammitic paragneiss, with conformable lenses of pelite, quartzite, and mafic gneiss, with subordinate intrusives. Metamorphosed to amphibolite facies. Unconformably overlain by Yandanooka Group.||||||
34432|Mullingarra Complex|44138|4|Described|p264 Fig.3-54, p265, p266, p272|||Muscovite from a pegmatite vein was dated at 1120 Ma (Wilson et al., 1960).|2.09 and 2.12 Ga (Sm-Nd model ages).|||Is overlain unconformably by Yandanooka Group.|Pelitic, semipelitic and quartzo-feldspathic gneiss with lenses of quartzite and amphibolite, with pegmatite veins.|
34432|Mullingarra Complex|50008|5|Briefly described|p48|||Gneissic Inlier. Granulite facies paragneiss and minor mafic gneiss, pegmatite, granite, and migmatite. Age of zircon populations given. Geological Province: Pinjarra Orogen.  Neoproterozoic?||||||08-APR-10
34432|Mullingarra Complex|50223|5|Briefly described|p344 Fig. 1, p356|Paleoproterozoic|Paleoproterozoic|Structural term in this context.  Age: 2.2Ga (Cobb et al, 2001).  Geological Province:  Perth Basin.||||||07-NOV-08
34432|Mullingarra Complex|60556|5|Briefly described|p2 Fig. 2|Proterozoic||||||||
34432|Mullingarra Complex|62113|5|Briefly described|p620.|Proterozoic|Proterozoic|Pinjarra Orogen.|||Includes Yandanooka Group.||Gneisses.|
34432|Mullingarra Complex|62381|5|Briefly described|p2 Fig.2, p9.|||Pinjarra Orogen. Northwest-directed compression c.1100-1000 Ma produced amphibolite- to granulite-facies assemblages.|||||Allochthonous blocks of metasedimentary gneiss.|01-JUL-14
34432|Mullingarra Complex|64161|6|Mentioned|p578 Fig.1|||||||||
34432|Mullingarra Complex|64635|6|Mentioned|p2 Fig.1, p5 Fig.4|||||||||
34432|Mullingarra Complex|64722|5|Briefly described|Fig. 2 p3-6, p19, 29||Paleoproterozoic|Of Pinjarra Orogen, WA. Thought to have been part of a block continuous with Northampton Complex. Contains a zircon with a 2181 +/- 10 Ma U-Pb crystallisation age; detrital zircons mostly 1900-1600 and 1400-1150 Ma.||||Unconformably overlain by Yandanooka Group.||11-APR-12
34432|Mullingarra Complex|64777|5|Briefly described|p1 Fig.2, p6 |||Paragneiss has detrital zircons with peaks at 1200, 1300-1450 and 1600-1800 Ma. Metamorphic zircons in gneisses have SHRIMP U-Pb ages of 1058 +/- 83 Ma (Cobb et al., 2001).|||||Consists of granulite facies paragneiss and minor mafic gneiss, pegmatite, granite, and migmatite or their equivalents.|
34432|Mullingarra Complex|65487|6|Mentioned|p2 Fig.1|||||||||
34432|Mullingarra Complex|65692|6|Mentioned|p25-26|||Part of the Pinjarra Orogen.|c.2.2 Ga (zircon; Cobb et al., 2001).|||||
34432|Mullingarra Complex|66299|6|Mentioned|p325.|||Not a stratigraphic unit; cf. Mullingarra Gneiss. Pinjarra Orogen. Interpreted as allochthonous terrane derived from Albany Fraser Belt. Emplaced in current position relative to Yilgarn Craton in Neoproterozoic.||||||
34432|Mullingarra Complex|67581|6|Mentioned|p37-39, 47-48|Mesoproterozoic|Mesoproterozoic|Pinjarra Orogen. Part of Perth Basin basement. Metamorphosed, deformed and intruded by granites and pegmatites between 1090-1020 Ma.||||||
34432|Mullingarra Complex|69595|6|Mentioned|p3 fig 1|||||||||
34432|Mullingarra Complex|70879|5|Briefly described|p1, p17-18|Mesoproterozoic|Mesoproterozoic|Northern Pinjarra Orogen. Protoliths aged 1100-1050 Ma are widespread. Has predominantly 1090-1020 Ma U-Pb zircon and monazite ages, consistent with the ages determined in this study.|||||Granitic and metasedimentary rocks.|
41891|Multicoloured Member""|12758|6|Mentioned|p16|Jurassic|Jurassic|Informal term for a member within the Cockleshell Gully Formation - originally used in unpublished WAPET Reports.  Term now abandoned - see Eneabba Formation.  Geological Province: Northern Perth Basin.||||||19-OCT-04
41891|Multicoloured Member""|23816|6|Mentioned|p240|||Informal name - refers to the Eneabba Member.||||||16-DEC-04
80471|Mulyu Dolomite|44142|5|Briefly described|p326 Tb.4-5|||1500m thick.||Uaroo Group.||Unconformably overlies Gascoyne Complex. Correlates with Cheyne Springs Formation.|Algal dolomite, quartz arenite.|
36889|Mumba Pelite|23525|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Parent: Moogie Metamorphics.||||||07-NOV-08
36889|Mumba Pelite|23527|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Moogie Metamorphics, Gascoyne Complex||||||07-NOV-08
36889|Mumba Pelite|23781|5|Briefly described|p61|||Of Moogie Metamorphics.||||||25-JAN-08
36889|Mumba Pelite|24544|4|Described|p10 Tb.1, p38|Paleoproterozoic|Archean|Age: >1800 Ma. Pelitic and psammitic schist. Of the Moogie Metamorphics. Unconformably overlain by Mount James Formation.||||||07-NOV-08
36889|Mumba Pelite|50218|5|Briefly described|p240 Fig.2, p247|||Of the Moogie Metamorphics. Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||07-FEB-11
36889|Mumba Pelite|50219|5|Briefly described|p260 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Moogie Metamorphics.  Geological Province: Glenburgh Terrane (Gascoyne Complex).||||||02-MAY-11
36889|Mumba Pelite|66299|6|Mentioned|p60.|||Named by Occhipinti and Sheppard (2001) for a belt of metapelitic rocks which included minor psammitic schist and quartzite. Subsequent mapping revealed psammitic schist as the main component, hence the name change to Mumba Psammite.||||||
36889|Mumba Pelite|67843|6|Mentioned|p6.|||Of Occhipinti and Sheppard (2001); subsequently Mumba Psammite. Commonly contains garnet and, locally, magnetite porphyroblasts.||||||
70373|Mundadjini member, lower|61716|5|Briefly described|p642|||Informal subdivision of the Mundadjini Formation. Composed primarily of beige coloured silicified sandstone with rare cross-beds - weathered to rounded blocks; several intervals of pebble conglomerate.||||||
70374|Mundadjini member, upper|61716|5|Briefly described|p642|||Informal subdivn. Med. to coarse-grained sandstone,dark-red to purplish; many beds have flaggy, bedding-planar fracture, some show ripple marks; high-angle x-bedding, several intervals of pebble conglomerate. Difficult to recognise due to silicification||||||19-MAY-06
34881|Mundajini Formation|22907|5|Briefly described|41|||Probable misspelling of Mudadjini Formation.||||||
34881|Mundajini Formation|24161|5|Briefly described|p11|||Of the Sunbeam Group. Correlated with the Skates Hills Formation.||||||
77458|Munderong Shale|67369|6|Mentioned|p251.|||A typo for Muderong Shale. The top of this unit was used as a seismic marker for interpreting the Pluto Field data.||||||
77458|Munderong Shale|67784|6|Mentioned|p28 table 1|||Misspelling of Muderong Shale.||||||
73505|Mundine Well Dolerite Suite|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: c. 755Ma. Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite.||||||
73505|Mundine Well Dolerite Suite|63420|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c.755Ma. Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrock; local syenite.||||||07-NOV-08
73505|Mundine Well Dolerite Suite|63441|5|Briefly described|p13 tb. 2|Neoproterozoic|Neoproterozoic|Of Wingate and Giddings (2000). Age: c.755Ma. Geological province: Pilbara Craton.||||||07-FEB-11
73505|Mundine Well Dolerite Suite|63469|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|Consists of dolerite dykes, sills, and small intrusions, also includes; minor quartz diorite, tonalite, and biotite monzogranite. Age dated at 755Ma.||||||24-JUN-13
73505|Mundine Well Dolerite Suite|63470|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: c. 755Ma. Dolerite dykes, sills and small intrusions; includes minor quartz diorite, trachyte and biotite monzogranite.||||||24-JUN-13
73505|Mundine Well Dolerite Suite|63471|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: c.755Ma. Dolerite dykes, sills and small intrusions; includes minor quartz diorite, tonalite and biotite monzogranite.||||||
73505|Mundine Well Dolerite Suite|64580|4|Described|map legend||Neoproterozoic|Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite.||||||15-DEC-08
73505|Mundine Well Dolerite Suite|64621|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: c.755Ma. Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite.||||||
73505|Mundine Well Dolerite Suite|64654|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Age: c. 755Ma. Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite.||||||12-DEC-12
73505|Mundine Well Dolerite Suite|64657|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Age: c. 755Ma. Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite; interpreted from aeromagnetic data where dashed.||||||26-NOV-08
73505|Mundine Well Dolerite Suite|65135|6|Mentioned|p17|Cryogenian|Cryogenian|~755 Ma||||||
73505|Mundine Well Dolerite Suite|65152|5|Briefly described|p3.|Neoproterozoic|Neoproterozoic|Dolerite dykes, c.755 Ma, intruding Gascoyne Complex and adjacent tectonic units. Cut by prominent dextral shear zones of 570 +/- 10Ma.||||||01-MAY-15
73505|Mundine Well Dolerite Suite|65453|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|Dolerite dykes, sills and small intrusions; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite. Age: c. 755 Ma (geochronology: Wingate, MTD and Giddings, JW. 2000).||||||
73505|Mundine Well Dolerite Suite|65829|5|Briefly described|p28.|Neoproterozoic|Neoproterozoic|Might be a conjugate set with the NW- to WNW-trending Round Hummock Dolerite Suite.|755 +/- 3 Ma (Wingate and Giddings 2000).|||||
73505|Mundine Well Dolerite Suite|65830|6|Mentioned|p27|Cryogenian|Cryogenian||755 Ma (Wingate and Giddings, 2000).|||||
73505|Mundine Well Dolerite Suite|65833|5|Briefly described|p17|Cryogenian|Cryogenian|755 Ma.||||||
73505|Mundine Well Dolerite Suite|66105|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Dolerite dykes, sills and small intrusions with abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite. Age: c.755 Ma (geochronology: Wingate, MTD and Giddings, JW. 2000).||||||
73505|Mundine Well Dolerite Suite|66108|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age shown as c.755 Ma. Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.||||||
73505|Mundine Well Dolerite Suite|66110|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age c.755 Ma. Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.||||||
73505|Mundine Well Dolerite Suite|66217|5|Briefly described|p5, p6 Table 1, p55.|Cryogenian|Cryogenian|NE-striking intrusions. Is younger than the Bangemall Group in the Bangemall Basin.|755 +/- 3 Ma.|||||
73505|Mundine Well Dolerite Suite|66299|4|Described|p6 Fig.3, p17, pp333-334.|Neoproterozoic|Neoproterozoic|Formerly referred to as the Mundine Well Suite (Hickman and Lipple 1978); later the Mundine Well dyke swarm (Wingate and Giddings 2000). A suite of dolerite dykes striking between north and north-northeast. Thickness mostly 5-25m, but ranges up to 150m; traceable along strike for tens of kilometres. Outcrops as boulders and tors among weathered rubble. Offset by dextral shear zones c.570 Ma.|755 +/- 3 Ma.|||Intrudes all the stratigraphic units in Gascoyne Province, and Wyloo Group, Capricorn Group and Bangemall Supergroup. Cuts across dykes of Narimbunna and Kulkatharra Dolerites.|Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Pilbara Province. Appears as Mundine Well Dolerite dyke. Produced in the Mundine Well Event, ME 28 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.755 Ma.|||||
73505|Mundine Well Dolerite Suite|66579|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||c.755 Ma.||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|66887|5|Briefly described|p5 Fig.4|Neoproterozoic|Neoproterozoic|Gascoyne Province.|~750 Ma estimated from Fig.4.|||||
73505|Mundine Well Dolerite Suite|66950|6|Mentioned|p9 Fig.8, p13|Cryogenian|Cryogenian||c. 755 Ma|||||
73505|Mundine Well Dolerite Suite|67247|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.755 Ma (Wingate and Giddings 2000).||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|67371|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.755 Ma (Wingate and Giddings 2000).||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|67373|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.755 Ma (Wingate and Giddings 2000).||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|67374|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.755 Ma (Wingate and Giddings 2000).||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|67375|5|Briefly described|p55.|Neoproterozoic|Neoproterozoic|Possibly contemporaneous with the Gairdner Dolerite.|755 Ma.|||||
73505|Mundine Well Dolerite Suite|67553|6|Mentioned|p57|Tonian|Tonian||755 Ma|||||
73505|Mundine Well Dolerite Suite|67843|5|Briefly described|p13.|Neoproterozoic|Neoproterozoic|Dykes of this unit are offset by dextral stike-slip faults dated at c.570 Ma (the Mulka Tectonic Event).|c.755 Ma.|||||
73505|Mundine Well Dolerite Suite|68281|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate and Giddings, 2000).||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|68282|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate and Giddings, 2000).||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|68283|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate and Giddings, 2000).||||Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrock; local syenite.|
73505|Mundine Well Dolerite Suite|68285|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate, Giddings, 2000)||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|68286|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate, Giddings, 2000)||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|68521|5|Briefly described|Map Legend|Cryogenian|Cryogenian|Geochronology from Wingate and Giddings (2000).|c. 755 Ma||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|68522|5|Briefly described|Map Legend|Cryogenian|Cryogenian|Geochronology from Wingate and Giddings (2000).|c.755 Ma||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|69003|5|Briefly described|p4, p48 Fig.57, p56, p59, p67|Neoproterozoic|Neoproterozoic|Capricorn Orogen. Also included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic. Offset dextrally by the c.570 Ma Mulka Tectonic Event.|c.755 Ma.||||Mafic dykes.|
73505|Mundine Well Dolerite Suite|69011|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate and Giddings, 2000)||||Comprises dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|69012|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c. 755 Ma (Wingate & Giddings, 2000)||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|29-APR-14
73505|Mundine Well Dolerite Suite|69013|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c.755 Ma (Wingate and Giddings, 2000)||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|30-APR-14
73505|Mundine Well Dolerite Suite|69015|5|Briefly described|Map Legend|Cryogenian|Cryogenian||c.755 Ma||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|02-MAY-14
73505|Mundine Well Dolerite Suite|69028|5|Briefly described|Map Legend|Cryogenian|Cryogenian|Gascoyne Province.|c. 755 Ma (Wingate and Giddings, 2000)||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|06-MAY-14
73505|Mundine Well Dolerite Suite|69080|6|Mentioned|p686 Fig.4|Cryogenian|Cryogenian||c.750 Ma.|||||
73505|Mundine Well Dolerite Suite|69091|6|Mentioned|p78|||NW Australia (Wingate and Giddings, 2000).|755 Ma|||||
73505|Mundine Well Dolerite Suite|69166|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite|
73505|Mundine Well Dolerite Suite|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|69185|4|Described|500k_geologyp08_lut.csv||Neoproterozoic|Geological Province: Pilbara Craton.|||||Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite|
73505|Mundine Well Dolerite Suite|69237|6|Mentioned|p2-3|||Appears as Mundine Dolerite Suite on p3.|755 Ma.|||||
73505|Mundine Well Dolerite Suite|69387|5|Briefly described|p8, p10, p13-22, p24, p50|Tonian|Tonian|Gascoyne Province, especially the NW part. Prominent NNE-trending features in aeromagnetic and photo mosaic images. Deformations discussed; structural fabric diagrams. SG and magnetic susceptibility values given.|c.755 Ma.|||||
73505|Mundine Well Dolerite Suite|69546|5|Briefly described|p101|Tonian|Tonian|Geological province: Gascoyne Province. Intruded into Gascoyne Province.|755 Ma|||||
73505|Mundine Well Dolerite Suite|69583|5|Briefly described|p58, p82, p133|Proterozoic|Proterozoic|Northern Yilgarn Craton.|c.755 Ma.|||||
73505|Mundine Well Dolerite Suite|69590|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic| See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|755 Ma (isotopic)||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite|
73505|Mundine Well Dolerite Suite|69596|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Gascoyne Province.||||||
73505|Mundine Well Dolerite Suite|69729|6|Mentioned|p85|Neoproterozoic|Neoproterozoic||c.755 Ma.|||||
73505|Mundine Well Dolerite Suite|70127|5|Briefly described|Map legend|Cryogenian|Cryogenian||c.755 Ma (Wingate and Giddings, 2000).||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|70138|5|Briefly described|Map legend.|Cryogenian|Cryogenian||||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|70795|4|Described|2_5m_interpdykel15_lut.csv|Tonian|Tonian|Also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv|755 Ma||||Dolerite dyke, sill or plug; small intrusions with local xenoliths and potassic alteration of wallrock.|
73505|Mundine Well Dolerite Suite|70814|6|Mentioned|p19||||c. 755 Ma|||||
73505|Mundine Well Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Tonian|Tonian|Gascoyne Province, Pilbara Craton.|755 Ma|||||20-MAY-20
73505|Mundine Well Dolerite Suite|70830|5|Briefly described|p22|Tonian|Tonian|Youanmi Terrane. |c. 755 Ma|||||
73505|Mundine Well Dolerite Suite|71000|6|Mentioned|p66|||||||||
73505|Mundine Well Dolerite Suite|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||dolerite, tonalite|
73505|Mundine Well Dolerite Suite|71273|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||c.755 Ma.||||Dolerite dykes, sills and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|71804|5|Briefly described|p392, p394-p395|||Capricorn Orogen. Geochronology results, interpretation and methodology are discussed.|c. 755 Ma||||Dolerite dykes.|
73505|Mundine Well Dolerite Suite|71869|6|Mentioned|p4|||Capricorn Orogen.||||||
73505|Mundine Well Dolerite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic||755+/-3 Ma||||Dolerite dykes, sills, and small intrusions with locally abundant xenoliths and potassic alteration of wallrocks; includes minor quartz diorite, syenite, tonalite, and biotite monzogranite.|
73505|Mundine Well Dolerite Suite|72238|5|Briefly described|p42-43|Tonian|Tonian||c. 755 Ma|||||
77221|Mundine Well Dolerite Swarm|66299|6|Mentioned|p242.|||Apparently a conflation of the invalid term 'Mundine Well dyke swarm' (Wingate and Giddings 2000) with the current 'Mundine Well Dolerite Suite'.||||||
36952|Mundine Well Suite|23585|6|Mentioned|p23|||||||||
36952|Mundine Well Suite|23757|6|Mentioned|p15|||Of Hickman (1983).  Age: 755+/-3Ma (SHRIMP U-Pb baddeleyite geochronology).||||||
36952|Mundine Well Suite|24353|5|Briefly described|p10 Tb.1|Cryogenian|Cryogenian|Age: 755Ma. Geological Province: Pilbara Craton||||||
36952|Mundine Well Suite|24531|6|Mentioned|p11 Tb. 2|||||||||
36952|Mundine Well Suite|50189|5|Briefly described|p26-27|Proterozoic|Proterozoic|Fine grained dolerite dykes intruding the granitoid complexes and the Warrawoona Group. Age: 755 +/- 3Ma (SHRIMP U-Pb baddeleyite).||||||
36952|Mundine Well Suite|50544|5|Briefly described|p16 Tb. 1, p61|Neoproterozoic|Neoproterozoic|Age: c. 775Ma (SHRIMP U-Pb baddeleyite, Wingate, 1997).||||||
36952|Mundine Well Suite|62129|6|Mentioned|p22|||||||||07-FEB-11
36952|Mundine Well Suite|65008|6|Mentioned|p24|||||||||
36952|Mundine Well Suite|66299|6|Mentioned|p333.|||Name used by Hickman and Lipple (1978) for a suite of ENE-trending dolerite dykes in the Pilbara region. Later referred to as the Mundine Well dyke swarm (Wingate and Giddings 2000); subsequently formalized as Mundine Well Dolerite Suite.||||||
36952|Mundine Well Suite|69299|5|Briefly described|p9 Tb.2, p20|||Intruding east-northeast trending dolerite dykes on COOYA POOYA are correlated with Mundine Well Suite of Hickman and Lipple (1975), dated at 755 Ma by Wingate and Giddings (2000).|755 Ma||||Dolerite dykes.|
34330|Mundine Well Suite""|22717|6|Mentioned|P11|||||||||
40093|Mundine Well dyke swarm|24115|5|Briefly described|p26|Cryogenian|Cryogenian|Age: 755 +/- 3 Ma.||||||
40093|Mundine Well dyke swarm|62381|6|Mentioned|p2 Fig.2.|||||||||01-JUL-14
40093|Mundine Well dyke swarm|62428|4|Described|p336|Neoproterozoic|Neoproterozoic|Dolerite dykes concentrated in the Gascoyne Complex and western parts of the Hamersley, Ashburton and Bangemall Basins. Age: 755Ma.||||||10-FEB-09
40093|Mundine Well dyke swarm|64936|5|Briefly described|map legend|Proterozoic|Proterozoic|Age: c. 755 Ma (geochronology: MTD Wingate and JW Giddins 2000). Dolerite dyke with locally abundant granitic xenoliths and potassic alteration of wallrocks; local syenite.||||||
40093|Mundine Well dyke swarm|65506|6|Mentioned|p988||755 Ma.|May cross-cut the Bangemall Supergroup.||||||
40093|Mundine Well dyke swarm|66299|6|Mentioned|p333.|||Term used by Wingate and Giddings (2000) for a suite of ENE-trending dolerite dykes in the Pilbara region; formerly known as Mundine Well Suite (Hickman and Lipple 1976); now formalized as Mundine Well Dolerite Suite.||||||
40093|Mundine Well dyke swarm|67581|6|Mentioned|p39, 47|||Appears as Mundine Well Dyke Swarm on p47. Intruded Yilgarn Craton.|755 Ma.|||Intruded Northampton Complex.||
40093|Mundine Well dyke swarm|71288|6|Mentioned|p136, 138|Neoproterozoic|Neoproterozoic|Paleopole positions from this unit locate Australia in low latitudes in the late Neoproterozoic. Presented as Mundine Dyke Swarms.|758-752 Ma.|||||
40093|Mundine Well dyke swarm|73184|6|Mentioned|p196|Tonian|Tonian|Yilgarn Craton, northwest margin and Pilbara Craton, west margin.|ca 755 Ma|||||
72355|Mundine Well dykes|65368|5|Briefly described|p13, 18|Cryogenian|Cryogenian|755 Ma (Wingate and Giddings 2000). High quality palaeomagnetic pole data available.||||||19-MAR-12
72355|Mundine Well dykes|69412|6|Mentioned|p1, 8||||755 Ma.|||||
23850|Mungada Group|41066|6|Mentioned|1 of 2 K05|||||||||
38963|Munganbrina Suite|23807|5|Briefly described|p113|||Geological Province: Pilbara Craton.||||||16-AUG-05
38963|Munganbrina Suite|24590|5|Briefly described|p40 Fig. 2.3|||Constitutes more than half of the Mount Edgar Granitoid Complex. Also presented in combination with Boodallana Suite. See also p42.||||||07-FEB-11
38963|Munganbrina Suite|50189|6|Mentioned|p7|Archean|Archean|Of Williams and Collins (1990). Superseded by Munganbrina Monzogranite.||||||07-NOV-08
38963|Munganbrina Suite|50544|5|Briefly described|p30|Archean|Archean|Superseded by Munganbrina Monzogranite (Williams, 1999).  Age: c.3241+/-3Ma (Nelson, 2000) on MOUNT EDGAR sheet further south.||||||07-NOV-08
38963|Munganbrina Suite|60429|6|Mentioned|p7|||Of Collins (1983,1993). Replaced by Munganbrina Monzogranite.||||||07-FEB-11
38963|Munganbrina Suite|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Replaced by Munganbrina Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
38963|Munganbrina Suite|65827|6|Mentioned|p25|Paleoarchean|Paleoarchean|Previously included Munganbrina Monzogranite.
||||||
38963|Munganbrina Suite|66217|6|Mentioned|p33.|||Of Collins (1983, 1993). Subsequently Munganbrina Monzogranite (p5, p33, p37).||||||
38963|Munganbrina Suite|69041|4|Described|p7-p8, p18-p19|Mesoarchean|Paleoarchean|Pilbara Craton. Extends across the northern section of the Mount Edgar Igneous Complex. Outcrop varies from rubble, scattered to abundant boulders, large tors, low slabs and gorges. Includes 9 unnamed subunits. The suite is weakly to strongly foliated and is intruded by abundant aplite, pegmatite veins and dykes. Monzogranite has a relatively moderate to high radiometric total count and moderate magnetic susceptibilites. The granodiorite and granite units have moderate radiometric total counts and very low to low magnetic susceptibilites.|3178 +/- 41 Ma (isochron, Collins & Gray, 1990)|||Intruded by the Chimingadgi Trondhjemite.|Fine- to coarse-grained, biotite monzogranite to biotite granodiorite and biotite-muscovite-garnet monzogranite.|21-JUN-19
27852|Mungari Granite|30900|4|Described|p70|||Lithology||||||
27852|Mungari Granite|31041|6|Mentioned|Fig. 1|||||||||
27852|Mungari Granite|31044|6|Mentioned|p229|||||||||
27852|Mungari Granite|35681|6|Mentioned|p43|||||||||
27852|Mungari Granite|36008|5|Briefly described|p1108|||||||||
27852|Mungari Granite|36566|6|Mentioned|Fig.1|||||||||
27852|Mungari Granite|37373|6|Mentioned|Table 2.V|||||||||
27852|Mungari Granite|41935|6|Mentioned|p10|||||||||
27852|Mungari Granite|42626|5|Briefly described|p38|||||||||
27852|Mungari Granite|43102|5|Briefly described|p5|||U-Pb zircon age of 2610 Ma.||||||
27852|Mungari Granite|46311|14|Not recorded|p.10|||(Equivalent of Horse Rocks Granite).||||||
27852|Mungari Granite|65834|6|Mentioned|p49-50|||Coolgardie Goldfield.||||||
28830|Mungari granite|30219|6|Mentioned|p220|||Age of emplacement 2620+-20m.y.||||||
28830|Mungari granite|31039|6|Mentioned|p130|||||||||
28830|Mungari granite|31224|6|Mentioned|p121|||||||||
28830|Mungari granite|35681|6|Mentioned|Table 2|||Radiometric ages.||||||
28830|Mungari granite|36566|6|Mentioned|p253|||||||||
28830|Mungari granite|37373|6|Mentioned|p72|||||||||
28830|Mungari granite|41771|6|Mentioned|Table 1|||||||||
77657|Mungari granitoid|68066|6|Mentioned|p28, p21 Tb. 1|Archean|Archean|Discussed in Oversby (1975). Southeast KALGOORLIE. Ages: (a) Rb-Sr (Turek, 1966); (b) Pb-Pb (Oversby, 1975). Granitoids within greenstone belts - synkinematic.|(a) 2585 +/- 35 Ma; (b) 2640 +/- 35 Ma.|||||
40081|Mungaroo Formation sandstones|24205|6|Mentioned|p250 Fig. 7|||Informal reference to the sandstones of the Mungaroo Formation.||||||
40082|Mungaroo sandstones|24205|6|Mentioned|p253|||Informal reference to the sandstones of the Mungaroo Formation.||||||
80566|Mungeroo Formation|71377|6|Mentioned|p89|Triassic|Triassic|North West Shelf, Perth Basin. [Misspelling of Mungaroo Formation]||||||10-AUG-18
77746|Munji Member|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||16-OCT-13
33168|Munni Munni Basic Complex|44478|14|Not recorded|map legend||Archean|||||||07-NOV-08
27853|Munni Munni Complex|22469|6|Mentioned|p19|||Pilbara Craton||||||
27853|Munni Munni Complex|22620|6|Mentioned|p196|||||||||
27853|Munni Munni Complex|22672|4|Described|P267||Archean|Age of unit is 2927+/-13 Ma||||||07-NOV-08
27853|Munni Munni Complex|22715|5|Briefly described|table7, p213,214|Archean|Archean|Thickness: 5430m.||||||07-NOV-08
27853|Munni Munni Complex|23135|6|Mentioned|p285|||||||||
27853|Munni Munni Complex|23570|5|Briefly described|p27|Archean|Archean|Age: 2925+/-16Ma.   Geological Province: Pilbara Craton.||||||07-NOV-08
27853|Munni Munni Complex|23743|5|Briefly described|p12|Archean|Archean|Age: c.2925 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
27853|Munni Munni Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
27853|Munni Munni Complex|24168|6|Mentioned|p639|||||||||
27853|Munni Munni Complex|24550|5|Briefly described|p40|Archean|Archean|Intrudes the Whundo Group and the Cheratta Granitoid Complex. Age: 2925+/-16Ma (Arndt et al, 1991).||||||07-FEB-11
27853|Munni Munni Complex|30566|4|Described|p1|||||||||
27853|Munni Munni Complex|30766|6|Mentioned|p20|||||||||
27853|Munni Munni Complex|35739|6|Mentioned|p13|||||||||
27853|Munni Munni Complex|39697|3|Fully described|p74|||||||||
27853|Munni Munni Complex|41594|6|Mentioned|p30|||||||||
27853|Munni Munni Complex|41982|4|Described|Table 1 P1780|||||||||
27853|Munni Munni Complex|42092|4|Described|p143|||See also Fig.1||||||
27853|Munni Munni Complex|42329|4|Described|p3|||||||||
27853|Munni Munni Complex|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
27853|Munni Munni Complex|42785|5|Briefly described|p270, Fig.4 p267|||age of 2925 +/- 16 Ma.||||||
27853|Munni Munni Complex|42840|4|Described|p289|||see also Fig.1 p290.||||||19-MAY-08
27853|Munni Munni Complex|43052|5|Briefly described|Fig.3.8|||||||||
27853|Munni Munni Complex|43597|14|Not recorded|p715||Archean|Age: 2925+/-16 Ma (U-Pb) (Late Archean)||||||07-NOV-08
27853|Munni Munni Complex|43689|4|Described|p163|||||||||
27853|Munni Munni Complex|43717|6|Mentioned|p1|||||||||
27853|Munni Munni Complex|43794|5|Briefly described|p320|||||||||
27853|Munni Munni Complex|44477|6|Mentioned|p.6||Archean|SF/50-6.||||||07-NOV-08
27853|Munni Munni Complex|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~2950-~2900 Ma estimated from Fig.11.|||||15-DEC-16
27853|Munni Munni Complex|70312|6|Mentioned|p2|||West Pilbara Block. Located c.48 km S of Roebourne. Total thickness of 5.5km; crops out over 80 km2.|||||A layered sequence of clinopyroxene, peridotite and gabbro.|
77789|Munni Munni intrusion|60498|6|Mentioned|p1020.|||No lithology was stated for the stratigraphic name. Pilbara Craton. Has relatively Cl-poor apatite composition, similar to other Western Australian intrusions such as in the East Kimberleys.||||||03-JAN-18
38539|Munni-Munni Complex|23813|5|Briefly described|p111|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34312|Munni-Munni intrusion|22676|6|Mentioned|p284|||Pilbara Block||||||
76080|Munya Sandstone|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Misspelt in legend. See Munyu Sandstone. Murraba Basin.||||||19-OCT-11
76080|Munya Sandstone|68733|6|Mentioned|p188|Neoproterozoic|Neoproterozoic|Age shown as Neoproterozoic(?)||Basal unit of the Redcliff Pound Group.||||05-DEC-17
76080|Munya Sandstone|69508|5|Briefly described|Map legend.|Neoproterozoic|Paleoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Medium- to coarse-grained, sugary, massive quartz sandstone; red-brown micaceous silty sandstone.|
77459|Murat Formation|12491|5|Briefly described|p453, p454-456 Figs7-9|||Deposited in a shallow sea in a pre-rift sag basin.||||Overlies Mungaroo Formation. Is overlain by Athol Formation.||06-NOV-14
77459|Murat Formation|13615|6|Mentioned|p82|||||||||
77459|Murat Formation|67369|6|Mentioned|p246 Fig.3. ||Early Jurassic|Dampier Sub-basin. Shown as Murat-Athol Fm. on the diagram for reasons of space.||||||
80419|Murchison Monzogranite|70020|4|Described|p131|||Geological province: Yilgarn Craton.||||Overlain unconformably by Shadow Well Formation/Gossan Hill Group.||
80419|Murchison Monzogranite|70270|6|Mentioned|p520 Fig. 3|||After Clifford, 1992 PhD. Murchison Province.||||||
80419|Murchison Monzogranite|71168|6|Mentioned|p13 fig 7|||Yilgarn Craton. Shown as overlain by Shadow Well Formation, Gossan Hill Group.||||||07-FEB-18
32613|Murdunna Gabbro|46311|14|Not recorded|p.11|||||||||
32613|Murdunna Gabbro|46316|14|Not recorded|p.11||Paleoproterozoic|Prominent dyke of Widgiemooltha Dyke Suite. Follows N edge of Lake Cowan.||||||07-NOV-08
36114|Murgoo gneiss|23441|5|Briefly described|p153|Archean|Archean|~3-2.9Ga||||||07-NOV-08
70749|Murial Range Sandstone|62453|6|Mentioned|p16|||Geological Province: Murraba (formerly Birrindudu) Basin.||||||
76058|Muroulli Basalt|66195|5|Briefly described|p605|Neoarchean|Mesoarchean|in the Polelle Group. Tholeiitic lavas. [misspelling of Murrouli Basalt]||||||13-MAR-12
41125|Murphy granite|24196|5|Briefly described|p73|Archean|Archean|Informal name. Age: ca. 2670 Ma (Black et al., 2002). Geological Province: Merolia Domain, Yilgarn Craton.||||||07-NOV-08
76775|Murraba Group|64733|6|Mentioned|p169 Fig.1|Neoproterozoic|Neoproterozoic|||||||
69741|Murray Range Peridotite|61341|5|Briefly described|Map legend|||Presented as the compound name Murray Range Pyroxenite/Peridotite.||||||
69740|Murray Range Pyroxenite|61341|5|Briefly described|Map legend|||Presented as the compound name Murray Range Pyroxenite/Peridotite.||||||
70172|Murray Range cumulates|44109|6|Mentioned|p84|||Informal reference to rocks of the Murray Range intrusion. ||||||
75276|Murrin Murrin Complex|65264|5|Briefly described|p10|||Geological province: Kurnalpi terrane.  Mafic to ultramafic extensive ponded komatiitic lava lake unit in which differentiation led to the forming of substantial olivine orthocumulates.||||||07-FEB-11
80420|Murrin Murrin Igneous Complex|71168|6|Mentioned|p33||||||||Dunitic and gabbroic sills.|
80194|Murrin Murrin Komatiite|67198|6|Mentioned|p49|||Also appears as Murrin Murrin komatiite on p48. Said to be the term for high-magnesian basalt within the Minerie Sequence.||||||
68128|Murrin greenstones|60416|5|Briefly described|p7|||Informal name.  Correspond to the Murrin greenstone belt of Griffin (1990).  Mainly felsic volcanic rocks, basalt and dolerite to the north; and to the south, comprise conglomerate and sandstone.||||||09-MAR-05
40353|Murrouli Formation|23922|5|Briefly described|p1234|Archean|Archean|Geological Province: Murchison-Southern Cross Terrane, Yilgarn Craton.  Of the Luke Creek Group.||||||07-NOV-08
76059|Murroulli dolerite|66195|5|Briefly described|p611 Fig.9|Neoarchean||Informal and mis-spelt variation on Murrouli Basalt or a separate reference to a dolerite in the same area?  ?intrudes the Polelle Group.|Age shown as 2792 +/- 5 Ma.|||||13-MAR-12
76059|Murroulli dolerite|67129|5|Briefly described|p55|Archean|Archean|Northern Murchison Domain, Youanmi Terrane.|2792 +/- 5 Ma.|||||
76059|Murroulli dolerite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Boodanoo Suite.||||
76059|Murroulli dolerite|71168|5|Briefly described|p7|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Boodanoo Suite||||
75370|Musgravian Gneiss|64722|5|Briefly described|p16-17, 27|Calymmian|Calymmian|Of Edgoose et al (2004). Of the Musgrave Orogen. Not clear if this is equivalent to, or part of, the Birksgate Complex. Formed in a collision-related environment. Contains mostly 1600-1540 Ma, but rare 1500 Ma, zircons.||||||
75370|Musgravian Gneiss|64745|5|Briefly described|p372, p373 Fig. 3, p374 Tab.1|Calymmian|Calymmian|Not a formal stratigraphic unit. Age: ca. 1.60-1.54 Ga (U-Pb SHRIMP). Geol Prov: Musgrave Province. Also known as Birksgate Complex (within Fregon Domain) or Olia gneiss (within Mulga Park Domain). Felsic composition. See also Musgravian Gneisses.||||||
75370|Musgravian Gneiss|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
75370|Musgravian Gneiss|70083|6|Mentioned|p206|||The oldest recognised lithology in the eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Birksgate Complex in the Fregon Subdomain (of the Inlier), and the Olia Gneiss in the Mulga Park Subdomain. A volcano-sedimentary sequence.|1600-1540 Ma (protoliths).||||Predominantly felsic orthogneiss, subordinate interlayered mafic units, and rare metapelite, quartzite and calc-silicate.|
75371|Musgravian Gneisses|64745|5|Briefly described|p372, p380-382|||Collective term referring to multiple gneisses of similar age. Magmatic/volcanic rocks (dominant felsic, subordinate mafic); subordinate metasediments (metapelite, quartzite layers, calcsilicates). Geol. Prov: Musgrave Province. See Musgravian Gneiss.||||||18-SEP-09
41463|Mussell Creek Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Used interchangeably with Mussell Creek Granodiorite.||||||07-NOV-08
41464|Mussell Creek Granodiorite|50437|6|Mentioned|p3.2|||Geological Province: Kimberley Region. Of the Paperbark Supersuite. Used interchanngeably with Mussell Creek Granite.||||||10-AUG-04
40568|Myalup Member|12758|5|Briefly described|p3 Fig. 3|Early Triassic|Early Triassic|Of the Lesueur Sandstone.  Fine, dark grey clastic sediments interbedded with sandstone.  Occurs transitionally between the Cattamarra C.M. above and the Wonnerup Member below.  Correlates with the Mungaroo Fm.  Geological Province: Southern Perth Basin.||||||
40568|Myalup Member|24443|5|Briefly described|Fig.31|Late Triassic|Late Triassic|Of Lesueur Sandstone. Conformably overlies Wonnerup Member. Conformably overlain by Eneabba Formation. Geological Province: Perth Basin.||||||
40568|Myalup Member|50107|5|Briefly described|Map legend|Triassic|Triassic|Of the Lesueur Sandstone.  Geological Province: Southern Perth Basin.||||||
40568|Myalup Member|67925|5|Briefly described|Ch2 p10 fig 4, Ch3 p8|Rhaetian|Carnian|||Lesueur Sandstone||Overlies the Wonnerup Member. Overlain by the Eneabba Formation.||
40568|Myalup Member|69029|5|Briefly described|p332|Rhaettian|Carnian|Of Perth Basin.||Unit of Lesueur Sandstone.||||
40568|Myalup Member|69182|5|Briefly described|Ch2 p9, Ch2 p45, Ch2 p51|Late Triassic|Middle Triassic|Perth Basin. ||Lesueur Sandstone||Overlain by the Wonnerup Member.|Estuarine shales.|
40568|Myalup Member|70097|5|Briefly described|p19 Fig.3|Toarcian|Carnian|Southern Perth Basin. Bunbury Trough.||Lesueur Sandstone||Overlies Wonnerup Member. Is overlain by Cattamarra Coal Measures.|Sandstone.|12-SEP-17
40568|Myalup Member|71377|5|Briefly described|p41|||Perth Basin. Superseded by the Yalgorup Member.||||||
40568|Myalup Member|71958|5|Briefly described|p34|Rhaetian|Carnian|Vlaming Sub-basin.||Lesueur Sandstone||Overlies the Wonnerup Member. Overlain by the Eneabba Formation.||
40316|N. gracilis sand|50024|5|Briefly described|p13|Early Jurassic|Early Jurassic|Informal name.  A fault bound structure of the Athol Formation.  Hosts recoverable oil.  Geological Province: Carnarvon Basin.||||||
28843|Nallanaring Ignimbrite|42785|5|Briefly described|Fig.5 P269|||||||||
36832|Nallanaring Member|23570|4|Described|p129|Archean|Archean|Of Jeerinah Formation. Supersedes Nallanaring Volcanic Member of Williams (1968).   Age: 2684+/-6Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
36832|Nallanaring Member|23575|5|Briefly described|Map Legend|Archean|Archean|Of Jeerinah Formation. Underlying unit Isabella Member. Geological Province: Hamersley Basin.||||||07-NOV-08
36832|Nallanaring Member|67201|5|Briefly described|p29 Fig.15|||Northern Fortescue Basin, Northwest Pilbara Sub-basin.||Jeerinah Formation||||
36832|Nallanaring Member|69301|5|Briefly described|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northwest Pilbara Sub-basin, Sequence 4. ||Jeerinah Formation||||
25320|Namban granite|40349|6|Mentioned|Fig.2|||||||||
28844|Nambeet formation|24449|5|Briefly described|p740|||Informal - see Nambeet Formation.  Geological Province: Canning Basin.||||||
28844|Nambeet formation|35119|6|Mentioned|p465|||||||||
28844|Nambeet formation|41215|6|Mentioned|p265|||||||||
28844|Nambeet formation|61139|5|Briefly described|p42|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
67869|Namuldi Member|24544|4|Described|p57 Fig.43|Archean|Archean|Of Marra Mamba Iron Formation. Overlies Jeerinah Formation. Overlain by MacLeod Member. Banded iron-formation. Geological Province: Hamersley Basin.||||||07-NOV-08
67869|Namuldi Member|73022|6|Mentioned|p5|||[Misspelling of Nammuldi Member?]||||||
38725|Nanarup Formation|24397|6|Mentioned|p240|||Current name is Nanarup Limestone Member.  Authors suggest that after further drilling the status may be revised to formation level.||||||
80610|Nanine Tonalite|70030|5|Briefly described|p191|||Geological province: Murchison Domain, Yilgarn Craton.||Unit of Annean Supersuite.||||
80610|Nanine Tonalite|70830|6|Mentioned|p8|||Murchison Domain.||Annean Supersuite||||
40203|Nannarup Limestone""|23817|5|Briefly described|p430|Tertiary|Tertiary|Superseded by the Nanarup Limestone Member (Cockbain 1968a).  Geological Province: Bremer Basin.||||||
40203|Nannarup Limestone""|71789|6|Mentioned|p100|||Of McTavish (1966).||||||
77467|Nannutarra Formation|12471|6|Mentioned|p475 Fig.2. |Early Cretaceous|Early Cretaceous|Mis-spelling of Nanutarra Formation. Deposited after continental break-up; formed a sub-horizontal blanket with Yarraloola Conglomerate over older strata.||||||
77467|Nannutarra Formation|13615|6|Mentioned|p18, p35|||Crops out on margins of Peedamullah Shelf.Not recognised in sub-surface.  Continental to shallow marine.||Of Barrow Group.||This plus Yaraloola Conglomerate likely time equivalent ot Flacourt Formation.||07-FEB-19
32758|Nannyarra Formation|1943|5|Briefly described|p386, p389 Fig. 14|Middle Devonian|Middle Devonian|||||Unconformably overlies Hamelin Formation in Quobba-1, Pendock-1A. Overlain by Gneudna Formation in Pendock-1A.||
32758|Nannyarra Formation|6943|6|Mentioned|p601, p602.|||Shown as Nannyarra Ss on p602.||||Unconformably overlies Coburn Formation. Is overlain by Gneudna Formation.||
32758|Nannyarra Formation|6944|5|Briefly described|p571, p576-577, p585 Table 1.|Middle Devonian|Middle Devonian|Givetian age. Southern Carnarvon Basin. Overlies unconformably Precambrian basement in the southeast and, disconformably, Paleozoic rocks in the southwest. Coarse progradational siliciclastic sequence with minor fine-grained interbeds.||||||23-SEP-15
32758|Nannyarra Formation|13615|6|Mentioned|p16|Devonian|Devonian|Of Iasky and Mory, 1999. Gascoyne Platform. See also Nannyarra Sandstone, same page.||||||01-MAY-19
25325|Nannyarra Greywacke|23815|4|Described|p275|Middle Devonian|Early Devonian|Geological Province: Carnarvon Basin. Overlying unit: Gneudna Formation (conformable). Underlying unit: Dirk Hartog Formation. Max. thickness: 60 m. Fossiliferous.||||||27-APR-05
25325|Nannyarra Greywacke|31055|4|Described|p588|||Devonian. Optics on feldspars.||||||
25325|Nannyarra Greywacke|31561|5|Briefly described|p33|||See also P34. Late Devonian||||||
25325|Nannyarra Greywacke|32619|6|Mentioned|p464|||Givetian||||||
25325|Nannyarra Greywacke|32648|6|Mentioned|p32|||Dev.||||||
25325|Nannyarra Greywacke|32865|4|Described|p477|||||||||
25325|Nannyarra Greywacke|33386|6|Mentioned|Fig.7|||||||||
25325|Nannyarra Greywacke|33453|4|Described|p69|||Devonian.||||||
25325|Nannyarra Greywacke|34484|6|Mentioned|Fig.1|||||||||
25325|Nannyarra Greywacke|36257|6|Mentioned|Table 2.1|||||||||
25325|Nannyarra Greywacke|36743|6|Mentioned|p40|||||||||
25325|Nannyarra Greywacke|36890|3|Fully described|p274|||||||||
25325|Nannyarra Greywacke|37295|6|Mentioned|p52|||||||||
25325|Nannyarra Greywacke|41589|6|Mentioned|p118|||||||||
25325|Nannyarra Greywacke|44344|14|Not recorded|p.5,24,opp.4, map||Devonian|(G50-1).||||||
25325|Nannyarra Greywacke|44345|14|Not recorded|map legend|||Middle? Devonian.||||||
25325|Nannyarra Greywacke|44537|14|Not recorded|map legend||Middle Devonian|Middle Devonian.||||||
25325|Nannyarra Greywacke|44657|14|Not recorded|p.5,7,8,17|||||||||
25325|Nannyarra Greywacke|45015|2|Defined|p34-39, map legend|Devonian|Devonian|Greywacke, quartzwacke and siltstone.  Unconformably overlies Tumblagooda Sandstone; conformably overlain by Gneudna Formation. Geological Province: Carnarvon Basin.||||||31-MAY-06
25325|Nannyarra Greywacke|45016|14|Not recorded|p.9 (map)|||||||||
25325|Nannyarra Greywacke|45041|6|Mentioned|Fig.45|||||||||
25325|Nannyarra Greywacke|45063|6|Mentioned|Fig. 9|||Devonian||||||
25325|Nannyarra Greywacke|46973|6|Mentioned|Fig.17|||||||||
25325|Nannyarra Greywacke|48628|14|Not recorded|p.4,6-8,15,16||Silurian|Fig.5. Overlies Dirk Hartog Limestone.  (F50-13/Wandagee). Age: ?Silurian.||||||
25325|Nannyarra Greywacke|61958|5|Briefly described|Map sheet 1|Devonian|Devonian|||||||
23862|Nanular Sandstone|22694|5|Briefly described|p8|||Edmund Subgroup, Bangemall Basin||||||
23862|Nanular Sandstone|22905|6|Mentioned|p54|||Not recognised on EDMUND sheet.||||||20-MAY-04
23862|Nanular Sandstone|22940|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Edmund Subgroup, Bangemall Basin. Underlying unit: Devil Creek Formation.||||||
23862|Nanular Sandstone|23485|6|Mentioned|p31|||Superseded by Nanular Member of the Ullawarra Formation.||||||
23862|Nanular Sandstone|24183|5|Briefly described|p4 Fig.3|Mesoproterozoic|Mesoproterozoic|Of the Dooley Subgroup (Chuck 1984)||||||
23862|Nanular Sandstone|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Now included in Ullawarra Formation. Of Dooley Subgroup.||||||
23862|Nanular Sandstone|40089|2|Defined|p31|Mesoproterozoic|Mesoproterozoic|||||||
23862|Nanular Sandstone|41360|6|Mentioned|p192|||||||||
23862|Nanular Sandstone|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23862|Nanular Sandstone|44142|4|Described|p313 Tb.4-4, p318-319|||Restricted to southern margin of Bangemall Basin between Mt Deveril and Mt Clara. Within Dooley Subgroup of Chuck (1984). 2200 m thick.||Edmund Subgroup.||Overlies Devil Creek Formation conformably. Is overlain by Ullawarra Formation.|Medium- to fine-grained quartz arenite, coarse grained quartz siltstone; interbeds shale, wacke.|
23862|Nanular Sandstone|50225|5|Briefly described|p387 Fig. 2|||Formerly of the Ullawarra Formation - now superseded?||||||07-FEB-11
28848|Nanyarra Sandstone|38770|5|Briefly described|p62|||Carnarvon Basin... Misspelling of Nannyarra Sandstone?||||||
28848|Nanyarra Sandstone|71146|5|Briefly described|p6|Eifelian|Eifelian|Southern Carnarvon Basin.||||Overlain by the Gneudna Formation.|Sandstone.|
41206|Nardoo granite|50222|6|Mentioned|p333 Tb. 2|Paleoproterozoic|Paleoproterozoic|Informal name.  Age: 1.97Ga (Occhipinti et al, 2004).  In the Glenburgh terrane.||||||07-NOV-08
70638|Nargun leucogranite|61252|5|Briefly described|p67 Tb.1|Archean|Archean|Informal name. Age: 3450+/-20 Ma. Of the Carlindi granitoid complex.||||||07-NOV-08
83191|Narimbunna dolerite|73056|6|Mentioned|p298|Calymmian|Calymmian||ca. 1465 Ma||||Mafic sills.|
27857|Narndee Complex|35469|6|Mentioned|p45|||||||||
27857|Narndee Complex|38492|4|Described|p78|||||||||
27857|Narndee Complex|40337|4|Described|p12|||||||||
27857|Narndee Complex|41594|6|Mentioned|p30|||||||||
27857|Narndee Complex|42019|6|Mentioned|p23|||||||||
27857|Narndee Complex|44149|4|Described|p13, p119-120, p124-125|Archean|Archean|Layered sequence estimated at 9 km thick. Layering rarely seen due to rubbly nature of outcrops.  The lower zone is 3.6km thick. The gabbronorite zone is 1800m thick. [The text deals with this unit in two parts: North and South, which are not regarded as separate stratigraphic units.]|||||Layered ultramafic sequence: dunite, peridotite, olivine pyroxenite, gabbro, gabbronorite, dolerite sills and dykes, granitoid stocks and dykes.|
83158|Narndee Intrusive Complex|72494|5|Briefly described|p22, 24, 30|||Mount Magnet area, Youanmi Terrane, Yilgarn Craton. Geochemistry plots.|c.2800 Ma.||||Hornblende-rich, wet magmas. Includes gabbros.|
76056|Narndee gabbro|66195|5|Briefly described|p611 Fig.9|Neoarchean|Mesoarchean|Informal reference to dated sample 191056 from the Narndee Igneous Complex.  ?intrudes the Norie Group. Age: 2800 +/- 6 Ma.||||||13-MAR-12
76056|Narndee gabbro|70020|5|Briefly described|p118|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton.||Unit of Boodanoo Suite.||||
76056|Narndee gabbro|71168|5|Briefly described|p7|Mesoarchean|Mesoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||Boodanoo Suite||||
24421|Narracoota Volcanics|7161|4|Described|p90, p92 Fig.4, p94|Orosirian||Minimum age determined using a Pb model age from an epigenetic Cu-Au-Ag ore deposit in the Narracoota Volcanics. Thickness may be between 2100-6000m.|1922 +/- 35 Ma|||Underlain by the Karalundi Formation. Overlain by the Johnson Cairn Shale.|Comprises subalkalic tholeiitic basalt and subvolcanic-dolerite, with tectonic signatures that straddle MORB, oceanic-island and continental settings.|
24421|Narracoota Volcanics|12099|6|Mentioned|p678 Fig.4, p681|||Superseded name. Parts included in the Narracoota Formation. Included in Glengarry Group by Gee (1987) and Gee and Grey (1993)||||||04-MAR-13
24421|Narracoota Volcanics|22493|6|Mentioned|p90|||||||||
24421|Narracoota Volcanics|23205|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|of Glengarry Sub Basin.||||||07-NOV-08
24421|Narracoota Volcanics|23747|6|Mentioned|p9|||Superseded by Narracoota Formation.||||||
24421|Narracoota Volcanics|23795|5|Briefly described|p3|Proterozoic|Proterozoic|Geological Province: Glengarry Basin.||||||
24421|Narracoota Volcanics|23798|5|Briefly described|p2|||See also Narracoota volcanics. Of the Bryah Group. Comprises a folded sequence of mafic and ultramafic rocks. Underlies Thaduna Greywacke. Geological Province: Yilgarn Craton.||||||05-JUL-06
24421|Narracoota Volcanics|24522|5|Briefly described|p78, p79 Fig. 1a|||Geological Province: Yilgarn Craton||||||
24421|Narracoota Volcanics|35975|3|Fully described|p102|||||||||
24421|Narracoota Volcanics|38994|5|Briefly described|p31|||||||||22-DEC-09
24421|Narracoota Volcanics|40297|4|Described|p113|||||||||
24421|Narracoota Volcanics|40937|6|Mentioned|p28|||||||||
24421|Narracoota Volcanics|40938|6|Mentioned|p11|||||||||
24421|Narracoota Volcanics|40989|4|Described|p21|||||||||
24421|Narracoota Volcanics|41991|5|Briefly described|p130|||||||||
24421|Narracoota Volcanics|42148|6|Mentioned|p693|||||||||
24421|Narracoota Volcanics|42260|6|Mentioned|p125|||||||||
24421|Narracoota Volcanics|42344|5|Briefly described|p54|||||||||
24421|Narracoota Volcanics|43069|5|Briefly described|p18|||of Glengarry Group.||||||21-FEB-17
24421|Narracoota Volcanics|43102|5|Briefly described|p23|||||||||
24421|Narracoota Volcanics|43561|6|Mentioned|p1436|||||||||
24421|Narracoota Volcanics|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1987, 1990). Of the former Glengarry Group. Superseded by Narracoota Formation now of the Bryah Group. ||||||
24421|Narracoota Volcanics|61217|5|Briefly described|p43 Fig. 2A, p45|||Of the Bryah Group. Probably misspelt - see Narracoota Formation. Comprise a folded sequence of mafic and ultramafic rocks - with a mafic sequence of albitised dolerite and basalt at the top.  Overlain by Thaduna Greywacke.||||||07-FEB-11
24421|Narracoota Volcanics|62094|5|Briefly described|p236|||Of Gee (1987). Now part of Killara Formation. Tholeiitic to calc-alkaline volcanic and subvolcanic sequence hosting agate.||||||21-FEB-17
24421|Narracoota Volcanics|62289|6|Mentioned|p4 Fig. 2|Palaeoproterozoic|Palaeoproterozoic|Gee (1987) and Gee and Grey (1993)||||||
24421|Narracoota Volcanics|64384|5|Briefly described|p78 Tb. 8, p82|||Of the Glengarry Group. Geological province: Glengarry Sub-basin. Tholeiitic basalt sequence.||||||07-FEB-11
24421|Narracoota Volcanics|65418|5|Briefly described|p169.|||Defined by Gee (1987, 1990) and Gee and Grey (1993). Subsequently replaced by Narracoota Formation (Pirajno and Occhipinti, 1995; Pirajno and Occhipinti, in prep.) which excludes the suite of mafic rock in the SE corner of the Peak Hill 1:250 000 map sheet and includes it in the Killara Formation.||||||21-FEB-17
24421|Narracoota Volcanics|65419|6|Mentioned|p19.|Paleoproterozoic|Paleoproterozoic|Of Gee and Grey (1993). Some volcanic rocks in this unit have been assigned to the Killara Formation.||||||
24421|Narracoota Volcanics|65913|6|Mentioned|p8.|||Name replaced by Narracoota Formation. Included rocks now assigned to the Killara Formation.||||||
24421|Narracoota Volcanics|67232|5|Briefly described|p30.|||Northern margin of Yilgarn Block. Hosts copper sulfide and gold mineralisation at the Doolgunna Cu-Au project. The tectonic environment is analogous to that of Woolianna Gabbro.||||||
24421|Narracoota Volcanics|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. Zero to 6km thick arkose-basalt-greywacke rift facies.||Glengarry Group||||
24421|Narracoota Volcanics|70804|5|Briefly described|p2|||Obsolete name, replaced by the Narracoota Formation of the Bryah Group. ||||||
41236|Narracoota formation|50226|5|Briefly described|p420|||Informal - see Narracoota Formation.  Of the Bryah Group.  Geological Province: Bryah Basin.||||||
68018|Narracoota volcanics|23798|6|Mentioned|p18|||Informal - see Narracoota Volcanics. Geological Province: Yilgarn Craton.||||||05-JUL-06
37094|Narryer Complex|23744|6|Mentioned|p21|||||||||
37094|Narryer Complex|66106|6|Mentioned|p43-45|||Was intruded by granites (at the S edge of the Jack Hills belt) at ~2.65 Ga, underwent a metamorphic event between ~2.75 Ga and ~2.6 Ga.||||||
37094|Narryer Complex|70500|6|Mentioned|p141|Eoarchean|Eoarchean|See also Narryer Gneiss (p126).||||||
28854|Narryer Gneiss|23151|6|Mentioned|p63|||||||||
28854|Narryer Gneiss|42579|5|Briefly described|p12|||Variation on Narryer Gneiss Complex.  See also Table 2, Fig.3.||||||
28854|Narryer Gneiss|65419|6|Mentioned|p4 Fig.1.|||||||||
28854|Narryer Gneiss|70022|6|Mentioned|p122 Fig.12|||Yilgarn Craton. U/Pb age and Hf isotope data diagram comparing zircons from this unit with those from Archean units in other continents.||||||
28854|Narryer Gneiss|70500|6|Mentioned|p126|Eoarchean|Eoarchean|See also Narryer Complex (p141).|3.65-3.30 Ga (Kemp et al., 2010).|||||
28854|Narryer Gneiss|72259|6|Mentioned|App. Tb.B||||||||Includes granite and biotite monzogranite.|
41207|Narryer complex|50222|6|Mentioned|p335|||Informal name.  More a structural term in this context.||||||
81991|Navajo Formation|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4|||East of Zuleika Shear, Ora Banda Domain.|||||Quartz rich cross bedded sandstone.|
77556|Navajo Supersequence|66936|5|Briefly described|p141.|Archean|Archean|250 m thick sequence previously included in the Kurrawang Supersequence. Interpreted to be an outlier of the Merougil Supersequence basin.||||Unconformably overlies Kalgoorlie Sequence. Is unconformably overlain by Kurrawang Supersequence.|Quartzofeldspathic sandstone and clast-supported cobble and boulder conglomerate.|
77556|Navajo Supersequence|73391|6|Mentioned|p179|||Krapez et al. (2008).||||Correlated with the Merougil Formation at Kambalda.||
39345|Navajo sandstone|24091|4|Described|p61|Archean|Archean|Informal local name. Age: 2657+/-4Ma. Geological Province: Yilgarn Craton.||||||07-NOV-08
39345|Navajo sandstone|73391|4|Described|p26, 49, 99-100, 102, 110, 194-195, 244|||Ora Banda Domain, Kalgoorlie Terrane. Referred to as ""Navajo sandstone member (likely belongs to Kurrawang Formation)"" on p179.|2657 +/- 4 Ma (MDA).|Kurrawang Formation.||Unconformably overlies Upper Black Flag Formation. Is overlain unconformably by Kurrawang Conglomerate.|Polymictic clasts in quartz-rich sandstone and wacke; local jaspilite chert.|
23867|Neale Beds|24244|6|Mentioned|p3|||Outcrops mapped as this unit in the central part of NEALE 1:250 000 sheet are now included in Kanpa Formation.||||||
23867|Neale Beds|38243|6|Mentioned|Fig.2|||||||||
23867|Neale Beds|38988|6|Mentioned|p18|||||||||
23867|Neale Beds|45149|3|Fully described|p25|||See also Table 1.||||||
23867|Neale Beds|46975|6|Mentioned|p83|||||||||
23867|Neale Beds|50204|6|Mentioned|p51|Neoproterozoic|Neoproterozoic|Of the Officer Basin. Outcrops mapped under this unit in central part of the Neale 1:250 000 sheet are now included in Kanpa Formation. ||||||
70750|Neale Beds''|62453|6|Mentioned|p32|||Informal, see Kanpa Formation.||||||
70751|Neale Formation''|62453|6|Mentioned|p32|||Informal, see Kanpa Formation.||||||
27519|Neale beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27519|Neale beds|39340|5|Briefly described|p359|||||||||
73603|Nebo-Babel Intrusion|63465|5|Briefly described|p552 Fig. 1, p555 Fig. 3b|||Hosts a platinum-element sulphide deposit. See also p558 Fig. 8, p560.||||||
32824|Negri Formation|48831|14|Not recorded|p.85|||||||||
82053|Neil Creek Granite|72437|5|Briefly described|p88|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Medium-grained biotite monzogranite.|10-NOV-20
79426|Nerrely Monzogranite|67201|6|Mentioned|p22 Fig.13|||In De Grey Superbasin. [misspelt Nerrely Leucogranite]||||||
79816|Never Can Tell Formation|69586|5|Briefly described|p10-11, p13|||Agnew-Lawlers area. Previously known locally as Lawlers Basalt. Probably represents several distinct plume-related magma batches. Hosts gold mineralisation (Cox Crusader and Deliver deposits).||||Is overlain by Agnew Komatiite. Equivalent to Lunnon Basalt.|Includes basalts which have a poddy outcrop style (remnant pillow structures); contains scattered flattened amygdales and irregular cavities.|
36902|Neville granodiorite|23383|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Neville Granodiorite.  Age: c.1860Ma.||||||07-NOV-08
83931|Nevoria Complex|70281|6|Mentioned|p458-459, 478|||Nevoria mine area, Norseman-Wiluna Fold Belt, Yilgarn Craton. Rb-Sr isotope data tabulated.|2634 +/- 4 Ma (Qiu et al., 1999).||||Pegmatite dykes and a zoned granite-pegmatite intrusion.|
33211|Newman Sub-Group|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
33211|Newman Sub-Group|61958|5|Briefly described|Map sheets 1 and  2|Artinskian|Artinskian|Includes: Madeline and Coyrie Formations, Bogadi and Mallens Greywackes, Warra warringa Formation and Bulgadoo Shale.||||||01-OCT-15
33212|Newman Sub-group|44532|14|Not recorded|p.7, map|||(G50-5).||||||
34377|Newman sequence|22682|6|Mentioned|p29|||||||||
25340|Newmarracarra Beds""|23816|6|Mentioned|p244|||Superseded by the "Newmarracarra Series" (Teichert, 1947).||||||
25340|Newmarracarra Beds""|36293|6|Mentioned|p151|||||||||
25340|Newmarracarra Beds""|36890|6|Mentioned|p244|||Renamed Newmarracarra Limestone||||||
31941|Newmarracarra limestone|43876|14|Not recorded|p581||Middle Jurassic|||||||
69177|Newton Felsic Formation|60623|4|Described|p28 Tb.1, p29|Archean|Archean|Lower part of the Black Flag Group. Mafic conglomerates, felsic and intermediate volcanics.||||||07-NOV-08
69386|Nexus porphyry|60979|5|Briefly described|p111 Fig.15, p112|||Informal term. Dacitic porphyry forming a prominent 150m thick unit. Geological Province: Yilgarn Craton.||||||
75504|Ngumban Sandstone Member|64630|6|Mentioned|p35 |||Of Carolyn Formation.||||||
40775|Niagara Layered Complex""|24494|6|Mentioned|p20|||Of Witt (1994)||||||
40775|Niagara Layered Complex""|65264|5|Briefly described|p23|||Of Witt (1994b). Informal name for a grouping of dolerite and cumulate-textured gabbronorite and gabbroic anorthosite on the MELITA map sheet.||||||07-FEB-11
39664|Nibil formation|24449|5|Briefly described|p745|||Informal - see Carribuddy Group.  Geological Province: Canning Basin.||||||
25342|Nickol River Formation""|39697|6|Mentioned|p16|||Lower part of Roebourne Group named by Williams (1968)||||||
68296|Nickol Well cherts|24095|6|Mentioned|p51|||Geological Province: Pilbara Block.||||||
68297|Nickol Well cherts""|24095|5|Briefly described|p46|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
81606|Nicol River Formation|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province, West Pilbara Superterrane, Pilbara Craton.||||Overthurst by Regal Formation. Underlain unconformably by Ruth Well Formation.||03-SEP-19
80322|Nifty Member|67202|5|Briefly described|p148-149, p166-169|||Anderson et al. (2001). Hosts the Nifty stratabound copper deposit (described in great detail). Conductivity described and imaged. Appears as "Nifty member" on p166, as Nifty member on p167 and p169, and as Nifty carbonate member on p169.||Broadhurst Formation.|||A strongly silicified, pyritic and carbonaceous black shale and dolomitic mudstone sequence.|
76140|Nifty Member""|65826|6|Mentioned|p18.|||Informal name for a copper-mineralized bed in the Nifty Cu-Pb-Zn mine in the Lamil map area of the Officer Basin.||||||
40499|Nifty member|23900|5|Briefly described|p1538, p1540 Fig.4|Proterozoic|Proterozoic|Included in the Broadhurst Formation. Geological Province: Paterson orogen. Informal - localised name for stratigraphy of a mine.||||||
73884|Nileman Formation|50095|6|Mentioned|p129||Late Silurian|Geological Province: Carnarvon Basin. WA. Contains Amydrotaxis sp. (conodont).||||||04-FEB-08
72414|Nilling beds|48823|6|Mentioned|p8 Fig. 1|||Supersedes Nilling Beds.||||||
69388|Nimary dacitic - rhyodacitic rocks|60979|5|Briefly described|p91 Fig.4|||Informal reference to rocks in the Lake Violet Sequence in the Jundee goldfields. Geological Province: Yilgarn Craton||||||10-DEC-08
69387|Nimary dacitic rocks|60979|5|Briefly described|p90|||A succession of deformed dacitic to rhyodacitic volcaniclastic rocks and shale, with subordinate chert, andesite and basalt lying west of the Lyon basalt in the Jundee goldfield area. Geological Province: Yilgarn Craton.||||||
31027|Nimingarra Formation|24184|5|Briefly described|p699 Fig.3|Archean|Archean|Overlying Unit: Cundaline Formation. Geological Province: Pilbara Craton. Age: <3443Ma||||||07-NOV-08
36839|Nimingarra Iron Formation|23415|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Geological province:  Pilbara Craton. Banded iron formation, jaspilite, banded and ferruginous chert, and black carbonaceous shale; metamorphosed.||||||07-NOV-08
36839|Nimingarra Iron Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Overlying unit Cundaline Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|23585|4|Described|p13|Archean|Archean|Of Gorge Creek Group. Overlain by Cundaline Formation. Underlain by Warrawagine Granitoid Complex. Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|23757|4|Described|p10-11|Archean|Archean|Of Gorge Creek Group. Thickness: 1000m. Geological Province: Pilbara Craton. Consists of BIF, jaspilite (banded hematite and red jasper), black and white banded and ferruginous chert, black (pyritiferous) shale and grey mudstone.||||||07-NOV-08
36839|Nimingarra Iron Formation|23783|5|Briefly described|p84|Archean|Archean|Of Gorge Creek Group.||||||07-NOV-08
36839|Nimingarra Iron Formation|24025|4|Described|p8 Tb. 1|Archean|Archean|Of Gorge Creek Group.  Banded iron formation, banded and ferruginous chert, black (pyritic) shale, mudstone.  Max. thickness: 1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Gorge Creek Group.   Geological Province: Pilbara Craton||||||07-NOV-08
36839|Nimingarra Iron Formation|50189|4|Described|p16, 28|Archean|Archean|Of the Gorge Creek Group. Replaced Cleaverville Formation in northern Pilbara Craton. Consists of BIF, Jasper, chert, shale and mudstone. Unconformably overlain by Hardey Formation. Max. Thickness: 1000m. Ages: 3458 +/- 18 to 3403 +/- 10Ma.||||||07-NOV-08
36839|Nimingarra Iron Formation|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group.  Overlies: Corboy Formation.  Underlies: Paradise Plains Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|50383|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton||||||07-NOV-08
36839|Nimingarra Iron Formation|50544|3|Fully described|p32, p19 Tb. 2 (amended)|Archean|Archean|Of the Gorge Creek Group.  BIF, jaspilite, banded chert, chery, basal conglomerate, sandstone, shale.  Contains hematite lodes.  Max. age: 3404+/-10Ma.  Max. thickness: 1000m.  See also p21 Tb. 4, p64.||||||07-NOV-08
36839|Nimingarra Iron Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup).   Banded iron-formation, jaspilite, banded and ferruginous chert, and black carbonaceous shale.  Age: <3235Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|60429|4|Described|p12, p16-17,  p36 Appdx. 1|Archean|Archean|This name has now been replaced in 2006 and absorbed into Cleaverville Fm. Of Gorge Creek Gp. Previously mapped as Cleaverville Fm in NE part of Pilbara Craton. Ages range: 3462+/-18 to 3362+/-13ma. See also p28.||||||07-FEB-11
36839|Nimingarra Iron Formation|60636|5|Briefly described|p35-36 Fig. 3.2|||Of the Gorge Creek Group. Banded iron formation, banded and ferruginous chert. See also p38 Fig. 3.3.||||||07-FEB-11
36839|Nimingarra Iron Formation|61253|5|Briefly described|p51|Archean|Archean|Of the Gorge Creek Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
36839|Nimingarra Iron Formation|62427|6|Mentioned|p3 Fig.2, p6 Fig.3|||||Unit in Gorge Creek Group.|||Banded iron formation, banded and ferruginous chert.|
36839|Nimingarra Iron Formation|63236|5|Briefly described|Map legend|Archean|Archean|Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation. Geological Province: east Pilbara-Greenstone Terrane.||||||07-NOV-08
36839|Nimingarra Iron Formation|63441|5|Briefly described|p6 Tb. 1, p26|Archean|Archean|Of Williams (1999). Formerly a formation of the Gorge Creek Group. Now redefined within Cleaverville Formation (Gorge Creek Group). This name now abandoned.||||||07-FEB-11
36839|Nimingarra Iron Formation|64628|6|Mentioned|p171 Fig.1. |||Coppin Gap greenstone belt, Pilbara Craton.||Unit in Gorge Creek Group.|||Coarse clastic sedimentary rock, BIF.|
36839|Nimingarra Iron Formation|64688|5|Briefly described|Map legend|Archaean|Archaean|Geological province: Pilbara Craton. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||
36839|Nimingarra Iron Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Gorge Creek Group.||Overlies Corboy Formation.|Black, blue, white and cream banded chert; ferruginous red, brown and yellow banded chert; weakly metamorphosed.|
36839|Nimingarra Iron Formation|67827|6|Mentioned|p417|||Northeast Pilbara.||||||
36839|Nimingarra Iron Formation|69167|6|Mentioned|143994.1.pdf|Archaean|Archaean|Age derived from basal quartz metasandstone sample (143994.1.pdf) that is interlayered with banded iron formation, chert and jasperlite.|3362 Ma +/- 13 Ma (SHRIMP)|||Overlain by Cundaline Formation||
36839|Nimingarra Iron 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.||||
36839|Nimingarra Iron Formation|69538|6|Mentioned|p533|Archean|Archean|Occurs at the Yarrie and Callawa plateaux. Source of Eel Creek Formation detrital iron deposit.||||||
36839|Nimingarra Iron Formation|69590|4|Described|143994.1.pdf + other geochron files|||Sample GSWA 143994 (quartzite) yielded an interpreted maximum depositional age of 3362+\-3 Ma of the sandstone protolith (weighted mean 207Pb/206Pb). Sample GSWA 143995 (quartzite) yielded an interpreted maximum depositional age of 3403+\-10 Ma of the sandstone protolith (weighted mean 207Pb/206Pb). |||||Quartz metasandstone interlayered with banded iron-formation chert and jasperlite.|
77216|Nimingarra Iron-Formation|66217|6|Mentioned|p41.|||Former name for rocks now included in Cleaverville Formation.||||||15-OCT-12
31127|Ninbing Formation|43482|6|Mentioned|23||Late Devonian|||||||
83179|Nindibillup dykes|73056|6|Mentioned|p293|Tonian|Tonian|Yilgarn Craton, central and southeast. WNW-trending dykes.|ca. 735 Ma|||||
83179|Nindibillup dykes|73057|6|Mentioned|p1, p4|Tonian|Tonian|Yilgarn Craton, central and southeast. WNW-trending dykes.|735 Ma||||Mafic dykes.|
25344|Ningbing group|41459|6|Mentioned|p278|||||||||
37992|Niobium Tuff""|22754|6|Mentioned|p20|||Informal name.  Forms basal part of Butchers Gully Member.  Max. thickness: 35m.||||||
37992|Niobium Tuff""|23383|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Informal name for mineralised portion of Butchers Gully Member (Olympio Formation).  Age: 1870 +/- 4Ma.||||||07-NOV-08
37992|Niobium Tuff""|64329|5|Briefly described|p15|||Fluorite-bearing rhyolitic volcaniclastic unit which hosts the Brockman deposit. Lowermost unit of a sequence of felsic lavas, subvolcanic rocks and volcaniclastic units within the Halls Creek Group.||||||
33868|Niobium tuff|22496|5|Briefly described|p7||Orosirian|c. 1870 Ma.  in Butchers Gully Member, Halls Creek Province||||||
40067|Niobium tuff""|22496|6|Mentioned|p7|||Contains c.1870Ma zircons.||||||12-AUG-04
40067|Niobium tuff""|24173|5|Briefly described|p9 Tb.1|Paleoproterozoic|Paleoproterozoic|Informal name.  See also niobium tuff and "niobium tuff". Overlain by Butchers Gully Member, of which it is a part.  Fine-grained strongly foliated rock with angular fragments of quartz, microcline and vesicular rock. Age: 1870 +/- 4Ma||||||07-NOV-08
39716|Nita formation, upper|24449|6|Mentioned|p746|||Informal - see Nita Formation.||||||
32782|Nob Well Intrusion|44229|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
32782|Nob Well Intrusion|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Warrawoona Group|||Serpentinized peridotite and metapyroxenite|
32782|Nob Well Intrusion|69185|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||||||
32782|Nob Well Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||serpentinite, pyroxenite|
32782|Nob Well Intrusion|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.||Warrawoona Group|||Serpentinized peridotite and metapyroxenite.|
26809|Nongra Beds|24197|5|Briefly described|p81|Paleoproterozoic|Paleoproterozoic|Of the Tanami Complex. Geological province: The Granites-Tanami Block.||||||07-FEB-11
26809|Nongra Beds|29804|4|Described|Table 1|||||||||
26809|Nongra Beds|29805|4|Described|Table 1|||||||||
26809|Nongra Beds|29809|6|Mentioned|Table 1|||||||||
26809|Nongra Beds|29811|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
26809|Nongra Beds|31361|4|Described|Table 2|||||||||
26809|Nongra Beds|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26809|Nongra Beds|42504|5|Briefly described|Table 3 P60|||||||||
26809|Nongra Beds|45140|2|Defined|p13-15, p18-19, p41, Appx.p4-5|Paleoproterozoic|Paleoproterozoic|Blake et al. (1975). The Granites-Tanami Block, W of the Ware Range and E and S of Birrindudu Range. Named after Nongra Lake. Reference area is at 19deg 42'50"S, 129deg 43'10"E, 48km SE of Birrindudu homestead, Birrindudu sheet area. Probably several thousand metres thick. Most outcrops are capped by laterite. Metamorphism, structure described.||Tanami Complex.||Is overlain unconformably by Gardiner Sandstone, Birrindudu Group and Antrim Plateau Volcanics.|Interbedded phyllitic shale, siltstone, greywacke and lithic arenite; banded chert; tuff, micaceous, medium- to fine-grained, with little to no quartz; acid porphyry.|
26809|Nongra Beds|46864|6|Mentioned|p37|||||||||
26809|Nongra Beds|48950|2|Defined|p19|Archean|Archean|||||||07-NOV-08
26809|Nongra Beds|50589|5|Briefly described|p1.1|||Geological Province: Granites-Tanami Block. Of the Tanami Complex.||||||
26809|Nongra Beds|69426|5|Briefly described|p11:5 Fig.11.4, 11:7|||Blake et al. (1975). Later incorporated into the Mount Winnecke Formation. Also appears as Nongra beds on p11:7, [mistakenly] attributed to Blake et al. (1975).||||Overlain by Pargee Sandstone.||12-JUL-16
68923|Noonkanbach Formation|60568|6|Mentioned|p387|Artinskian|Artinskian|Probable misspelling of Noonkanbah. Contains bryozoans.||||||27-FEB-09
80354|Noonkanbah Series|70774|5|Briefly described|p8|||Initial name of Wade (1936) that was renamed the Noonkanbah Shale in subsequent work before being finally revised as the Noonkanbah Formation.||||||
80355|Noonkanbah Shale|70774|5|Briefly described|p8|||Of Guppy et al. 1950. Revised from the Noonkanbah Series, this name is now obsolete after being renamed the Noonkanbah Formation by Guppy et al., 1951.||||||05-FEB-18
29957|Noreena Shale""|43055|6|Mentioned|p25|||Superseded by Balfour Formation||||||
33039|Nornalup Supersuite|24197|5|Briefly described|p22, p52|Mesoproterozoic|Mesoproterozoic|Example of the Kalkadoon Association. Dominated by heterogeneous ortho- and paragneisses; includes mafic enclaves. Age: 1190Ma, but appears to include granites of two ages, both 1190Ma and 1300Ma. Geological province: Albany Fraser Province.||||||07-FEB-11
33039|Nornalup Supersuite|50434|5|Briefly described|p1.1, 1.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Albany-Fraser Province. Age: 1170-1300Ma.||||||
83153|Nornalyup Gneiss|72491|6|Mentioned|p2|Ectasian|Ectasian|||||||
25349|Norseman Limestone|14227|5|Briefly described|Enclos. 2|Lutetian|Lutetian|Of Plantagenet Group. Presented as Norseman LST.||||||07-FEB-11
25349|Norseman Limestone|23331|5|Briefly described|1089|Middle Eocene|Middle Eocene|||||||
25349|Norseman Limestone|23533|5|Briefly described|p564 Fig 3|Late Eocene|Middle Eocene|Geological Province: Bremer Basin.||||||
25349|Norseman Limestone|23584|5|Briefly described|p31 Fig 17|Middle Eocene|Middle Eocene|||||||
25349|Norseman Limestone|23797|5|Briefly described|p3|||Underlies Redmine Group. Max Thickness: ~37m. Geological Province: Yilgarn Craton.||||||17-FEB-05
25349|Norseman Limestone|23817|5|Briefly described|p430|Late Eocene|Late Eocene|Geological Province: Bremer Basin.  Of the Eundynie Group.  Max. Thickness: 9.1m.  Fossiliferous.||||||
25349|Norseman Limestone|23989|5|Briefly described|p54 Fig. 46|Middle Eocene|Middle Eocene|Geological Province: Yilgarn Craton||||||
25349|Norseman Limestone|24165|5|Briefly described|p74|Eocene|Eocene|Lake Cowan-Buldania Rocks district. Fossil fauna listed.|||||Sandy fossiliferous limestone, fine-grained fossiliferous sandstone, and fossiliferous mudstone.|
25349|Norseman Limestone|24397|6|Mentioned|p239|||Superseded by Norseman Formation.  Geological Province: Eucla Basin.||||||
25349|Norseman Limestone|29601|6|Mentioned|p82|||||||||
25349|Norseman Limestone|30144|6|Mentioned|p84|||Foraminifera of Late Eocene age.||||||
25349|Norseman Limestone|30268|6|Mentioned|p44|||||||||
25349|Norseman Limestone|30562|4|Described|p19|||See also P6. Tertiary age||||||
25349|Norseman Limestone|30959|6|Mentioned|Map legend|Eocene|Eocene|||||||
25349|Norseman Limestone|31049|6|Mentioned|p393|||See also P394||||||
25349|Norseman Limestone|31051|6|Mentioned|p83|||See also Fig. 1||||||
25349|Norseman Limestone|31053|6|Mentioned|Fig. 1|||||||||
25349|Norseman Limestone|32552|6|Mentioned|p66|||See also P74, 192.||||||
25349|Norseman Limestone|32648|6|Mentioned|p32|||Eocene||||||
25349|Norseman Limestone|36890|3|Fully described|p430|||||||||
25349|Norseman Limestone|38773|6|Mentioned|p46|||||||||
25349|Norseman Limestone|39173|6|Mentioned|p325|||||||||
25349|Norseman Limestone|40877|5|Briefly described|p55|||||||||
25349|Norseman Limestone|41771|6|Mentioned|p49|||See also Fig.6||||||
25349|Norseman Limestone|42108|5|Briefly described|p322|||See also Fig.6||||||
25349|Norseman Limestone|42817|5|Briefly described|p29|||of Eundynie Group||||||
25349|Norseman Limestone|42959|5|Briefly described|p58|||see also p58 Fig.3||||||
25349|Norseman Limestone|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|||||||
25349|Norseman Limestone|43280|6|Mentioned|Map Legend||Tertiary|||||||
25349|Norseman Limestone|43838|4|Described|p4, Fig2 p6, 9||Tertiary|Interfingers with Werrilup Formation in Cowan Palaeodrainage. 37m thick.||||||12-JUL-16
25349|Norseman Limestone|65194|5|Briefly described|p135, p136 Fig.4.37, p138 Fig.4.38|Late Eocene|Middle Eocene|Fossiliferous, lithologically variable and partially dolomitised marine sediments in Cowan Palaeovalley. Overlies part of Werrillup Formation and is itself overlain by later-stage Werrillup Formation.||||||
25349|Norseman Limestone|65260|6|Mentioned|p27|Upper Eocene|Middle Eocene|Similar to a limestone unit in upper Hampton Sandstone. Also referred to as Norseman Formation in Fig.20 on the same page.||||||
25349|Norseman Limestone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Bremer and West Eucla Basins. Bartonian in age.||||||
25349|Norseman Limestone|69648|6|Mentioned|p24|||Proximal occurrences of Eocene limestone (namely Norseman Limestone) occur on west side of Eucla Basin, in tributary of Lefroy Palaeoriver (Gregory, 1916; Clarke, 1994). See Paling Member on OOLDEA.||||||
25349|Norseman Limestone|71788|14|Not recorded|p97-98, Plate 41 ||Late Eocene|Upper Eocene||||||
25349|Norseman Limestone|71789|6|Mentioned|p100|||Of Eundynie Group.||||||
69634|Norseman Limestone Formation|61155|5|Briefly described|p17|Middle Eocene|Middle Eocene|Of the Plantagenet Group and/or? Eundynie Group [which??]. Age: 45.5-43Ma.  Thickness in Norseman region: 30m. Geological Province: Bremer Basin and Norseman region.||||||
40330|Norseman granites|23924|6|Mentioned|p217 Fig. 9|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
67874|Norseman greenstones|60076|4|Described|p14-15|Archean|Archean|Informal name for grouping of greenstones in south Kambalda and Coolgardie domains.||||||07-NOV-08
70612|North End Dolerite|62406|6|Mentioned|p55|||Probably an informally named part of the Williamstown Dolerite in the Golden Mile?  Hosts the mature Mount Charlotte stockwork orebody.  In the Kalgoorlie gold belt.||||||
34340|North Head Limestone""|22718|6|Mentioned|P9|||||||||
83078|North Pole Basalt|73160|6|Mentioned|p9|||Misspelling of North Star Basalt? 3249 +/- 15 Ma Ar/Ar age associated with main hydrothermal event, 3061 +/- 18 Ma age represents a distinct, minor hydrothermal/thermal event, third hydrothermal/thermal event at 2294 +/- 14 Ma.||||||
40190|North Pole Chert|24182|5|Briefly described|p93 Fig. 3.|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
40190|North Pole Chert|73160|4|Described|p1-6, p10-16|Paleoarchean|Paleoarchean|Pilbara Craton, East Pilbara Terrane. Lowermost member of the Dresser Formation, thickness of 1 to 290 m. Also known as the Lower Chert Member. Deposited in a tectonically active volcanic caldera setting. Deposition varied up-section from deep water marine, through shallow marine to sub-aerial, and back to deep water marine environments, strongly influenced by syn-depositional hydrothermal activity. Hosts wrinkly, laminated, conical, and domical stromatolites within centimeter-thick dolomite-sulfide-chert beds. Contains hydrothermal silica and barite veins, dominantly orientated perpendicular to bedding. Referred to as Unit I by Terabayashi et al., (2003). Also shown as North Pole Chert Member p15.||Dresser Formation||Conformably overlies North Star Basalt.|Complex and variable association of bedded cherts (locally jaspilitic) interbedded with carbonate, sandstone, conglomerate, minor felsic volcaniclastic rocks, siliceous hot spring sinter deposits, coarse crystalline barite, stromatolites.|08-MAR-22
23879|North Rankin Beds|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
23879|North Rankin Beds|36112|5|Briefly described|p29|||||||||
23879|North Rankin Beds|41444|6|Mentioned|Fig.6|||||||||
23879|North Rankin Beds|42615|6|Mentioned|p28|||Superseded by North Rankin Formation||||||
23879|North Rankin Beds|43712|5|Briefly described|p10|Sinemurian|Hettangian|||||||
23879|North Rankin Beds|43722|5|Briefly described|p10|Sinemurian|Hettangian|||||||
23879|North Rankin Beds|43826|6|Mentioned|Fig.2,p163||Early Jurassic|||||||01-MAR-10
23879|North Rankin Beds|67368|5|Briefly described|p209 Fig.4, p210 Fig.5, p216, p217. |Early Jurassic|Early Jurassic|Has gas- and water-bearing sands. Is juxtaposed, across the major North Rankin Field bounding fault, against the Legendre Formation.||||Overlies Brigadier Formation. Is overlain by Murat Siltstone.||
77439|North Rankin beds|60379|6|Mentioned|p126 fig 3|Pliensbachian|Sinemurian|Dampier sub-basin, Carnarvon Basin||||||
77439|North Rankin beds|60386|6|Mentioned|p300|Early Jurassic|Late Triassic|Northern Carnarvon Basin. Deltaic-nearshore-shelf.||||||
33900|North Shaw regional suite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3470 Ma||||||07-NOV-08
70639|North Shaw suite|61252|6|Mentioned|p67 Tb.1|||Of the Shaw granitoid complex.||||||16-JUN-06
38604|North Shaw tonalite|23783|5|Briefly described|p115 Fig. 64|||Informal.||||||
38604|North Shaw tonalite|50427|6|Mentioned|p188 Fig.9|Archean|Archean|Informal.||||||07-NOV-08
35558|North Star Basalt Formation|23255|5|Briefly described|p47||Archean|Variation of North Star Basalt. Age: Sm-Nd whole rock isochron method at 3560+/-32Ma.||||||07-NOV-08
77522|North Star Formation|64628|6|Mentioned|p170.|Early Archean|Early Archean|||Unit in Warrawoona Group.||||
80098|Northampton Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Tonian|Tonian|Northampton Inlier.|c. 748 Ma|||||26-SEP-17
38816|Northampton Metamorphic Complex|23994|5|Briefly described|p159 Fig.4|Proterozoic|Proterozoic|||||||
83182|Northampton dykes|73057|6|Mentioned|p4|Tonian|Tonian|Yilgarn Craton, far west. NNE-trending dykes.|ca. 750 Ma|||||
68065|Northampton paragneiss|24526|6|Mentioned|p114|||Informal name  referring to gneiss within the Northampton Complex.||||||
38967|Northern Suite|23807|6|Mentioned|p131|||Geological Province: Pilbara Craton.||||||
38967|Northern Suite|24590|5|Briefly described|p42, p63|Archean|Archean|Northern part of the Corunna Downs Graniotid Suite. Granodiorite. See also p43 Fig. 2.4b.||||||07-FEB-11
38675|Northhampton Complex|23788|5|Briefly described|p5|||||||||
38675|Northhampton Complex|50620|6|Mentioned|p22|||Of the Pinjarra Orogeny. Age: 1000ma (Nelson, 1996, 1999, 2000, 2001 and 2002).||||||
38675|Northhampton Complex|60556|5|Briefly described|p2 Fig. 2|Proterozoic||||||||
25351|Norton Greywacke|31561|6|Mentioned|p7|||Artinskian||||||
25351|Norton Greywacke|33710|6|Mentioned|p120|||Brachiopods.||||||
25351|Norton Greywacke|34532|6|Mentioned|p225|||Byro Gp.||||||
25351|Norton Greywacke|35282|6|Mentioned|p39|||||||||
25351|Norton Greywacke|37295|6|Mentioned|Table 2|||||||||
25351|Norton Greywacke|39267|6|Mentioned|p248|||[Originally entered for NSW. CEBMar95]||||||
25351|Norton Greywacke|39974|6|Mentioned|p113|||||||||
25351|Norton Greywacke|44344|14|Not recorded|p.14-16,22,24||Artinskian|Fm of Minilya Subgroup (Byro Group). U.Artinskian. (G50-1). opp.4, map.||||||
25351|Norton Greywacke|44345|14|Not recorded|map legend||Artinskian|Artinskian.||||||
25351|Norton Greywacke|44372|6|Mentioned|p12|||||||||
25351|Norton Greywacke|44537|14|Not recorded|map legend||Artinskian|||||||
25351|Norton Greywacke|44657|14|Not recorded|p.5,6,9,10|||||||||
25351|Norton Greywacke|44994|6|Mentioned|Fig.7|||Equiv. Nalbia Gwk.||||||
25351|Norton Greywacke|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||31-MAY-06
25351|Norton Greywacke|45016|2|Defined|p170-178||Artinskian|Tb, p.124,125,137,155,157,163,166,167,181,184. (G50-1, type,F50-13).||||||
25351|Norton Greywacke|48831|14|Not recorded|p.74,76|||||||||
25351|Norton Greywacke|48858|14|Not recorded|p.4-15|||(G50-1/Norton). Pl.1,2.||||||
25351|Norton Greywacke|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||
39226|Norton metagabbro|23897|5|Briefly described|p377 Fig.1|||Informal name.||||||
39226|Norton metagabbro|60498|5|Briefly described|p1016 Fig.1, pp1017-1018.|Paleoproterozoic|Paleoproterozoic|Electron microprobe geochemical analyses of apatites are detailed.||Unit in Tickalara Metamorphics.|||Hornblende metagabbro and hornblende-magnetite metagabbro.|
79552|Nulchara Granite|67128|6|Mentioned|p3|||Musgrave Ranges. Appears as "The Angatja, Michell Nob, and Nulchara granites". [Formal name in the Database is Nulchara Charnockite].||||||
37215|Nullabor limestone|23989|5|Briefly described|p54 Fig. 46|Cenozoic|Cenozoic|Informal name. Geological Province: Yilgarn Craton||||||19-NOV-08
81607|Nullagaine Group|72251|6|Mentioned|p52|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of De Grey Superbasin.|3051-2930 Ma|||||
28878|Nullagine Conglomerate|45086|6|Mentioned|p23|||||||||
26812|Nullagine Formation|23570|6|Mentioned|p21|||||||||
26812|Nullagine Formation|36882|6|Mentioned|p124|||||||||
26812|Nullagine Formation|42345|5|Briefly described|p74|Paleoproterozoic||||||||07-NOV-08
32024|Nullagine Lavas|30704|5|Briefly described|p59|||||||||
32024|Nullagine Lavas|43870|14|Not recorded|p296,317|||Palaeomagnetic readings.  21S 120E.||||||
32024|Nullagine Lavas|45923|14|Not recorded|p.122|||||||||
32024|Nullagine Lavas|67027|6|Mentioned|p350.|||Pilbara.||||||
76837|Nullagine Volcanics|67027|6|Mentioned|p350.|||Included in the Fortescue Volcanics.||||||
32639|Nullagine conglomerates|45923|14|Not recorded|p135|||Gold.Quote of Maitland 1905.||||||
33169|Nullagine dolomite|44479|2|Defined|p.3|||E/51-1.||||||
38093|Nullagine"" Beds|23570|5|Briefly described|p11|Archean|Archean|Informal.  Geological Province: Pilbara Craton||||||07-NOV-08
39306|Nullara Carbonates|24377|5|Briefly described|p13|||Geological Province: Canning Basin||||||02-MAR-05
42465|Nullara Group|60702|5|Briefly described|p4|Late Devonian|Late Devonian|Platform sediments over the Lennard Shelf.  Geological Province: Canning Basin.||||||
38837|Nullara Limestone""|24061|5|Briefly described|p180|||Informal name. Geological Province:  Canning Basin.||||||
77575|Nullara Oolite|66127|6|Mentioned|p48.|||Of Smith et al. (1957); revised to Nullara Limestone by Playford and Cockbain (1976) for Famennian back-reef and bank subfacies of the platform facies. ||||||
69142|Nullara limestone|61139|5|Briefly described|p41|Late Devonian|Late Devonian|Geological Province: Canning Basin.||||||09-JUN-05
32578|Nulsen Slate|45543|4|Described|p.102||Archean|Unit of Woolyeenyer Group.||||||07-NOV-08
26084|Numbana Granite|23784|5|Briefly described|p42 Fig. 17|||Of Yule Granitoid Complex.||||||
26084|Numbana Granite|31308|6|Mentioned|Fig. 36|||||||||
26084|Numbana Granite|37633|5|Briefly described|Plate 5|||See also Plate 1 and P34.||||||
26084|Numbana Granite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
26084|Numbana Granite|39697|3|Fully described|p37|||See also P28||||||
26084|Numbana Granite|44150|5|Briefly described|p143 Tb.2-21, p149 Fig.2-137|||500 sq. km. Post-tectonic granitoid.||Yule Granitoid Complex|||Foliated syenogranite, marginal pegmatite. Sn, Ta, Be  in associated pegmatite present in greenstones.|
26084|Numbana Granite|50542|5|Briefly described|p108, p109 Fig. 57|Archean|Archean|Of the Yule Granitoid Complex. Age 2830-2890 Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
26084|Numbana Granite|63441|5|Briefly described|p12 Tb. 2|Archean|Archean|Superseded by Numbana Monzogranite (Split Rock Supersuite).||||||07-FEB-11
39765|Numbana pegmatite|24193|5|Briefly described|p890|Archean|Archean|Parent: Numbana Monzogranite. Geological Province: Pilbara Craton.||||||07-NOV-08
36338|Nummaldi Member|22689|6|Mentioned|Fig. 1 p138|||Of Marra Mamba Iron Formation. Misspelling of Nammuldi Member.||||||
32768|Nunnery Formation|44532|14|Not recorded|p.7, map|||(G50-5).||||||
32768|Nunnery Formation|45016|14|Not recorded|Fig. 65|||||||||
32768|Nunnery Formation|48885|14|Not recorded|p.10|||(G/50-6).||||||
29814|Nura Member|43050|5|Briefly described|p47|||Misspelling of Nura Nura Member of Poole Sandstone?||||||
80356|Nura Nura Limestone|70774|5|Briefly described|p7|||This was the first proposed sub-division of the Poole Sandstone by Wade (1936) before being renamed the Nura Nura Member by Guppy et al., 1951.||||||05-FEB-20
25357|Nura Nura member|37549|6|Mentioned|Fig.6|||||||||
25357|Nura Nura member|42017|6|Mentioned|p1|||||||||
80499|Nyalassy Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1859 Ma|Paperbark Supersuite||||
27865|Nymerina Basalt|22701|5|Briefly described|Fig2,p39|Archean||Fortescue Group, Hamersley Basin. Overlain by Jeerinah Formation.||||||07-NOV-08
27865|Nymerina Basalt|23570|5|Briefly described|p123|||See also Nymerina Basalt Member and Maddina Basalt.  Unit is combined with Maddina Basalt and Kuruna Siltstone of Hickman (1978) and referred to as Maddina Formation in this publication. Geological Province: Pilbara Craton||||||
27865|Nymerina Basalt|23585|5|Briefly described|p14 Fig 5|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
27865|Nymerina Basalt|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Fortescue Group.  Age: c.2.76-2.69Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
27865|Nymerina Basalt|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.76-2.69 Ga. Geological Province: Pilbara Craton. Parent: Fortescue Group. Overlying Unit: Kuruna Siltstone. Underlying Unit: Tumbiana Formation.||||||07-NOV-08
27865|Nymerina Basalt|24353|4|Described|p5, 26|Archean|Archean|Not a current name. Now included in the Maddina Basalt. Overlying Unit: Kuruna Siltstone. Parent: Maddina Basalt. Geological Province: Pilbara Craton||||||07-NOV-08
27865|Nymerina Basalt|31307|6|Mentioned|p80|||||||||
27865|Nymerina Basalt|31853|6|Mentioned|p63|||||||||
27865|Nymerina Basalt|35641|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27865|Nymerina Basalt|36551|6|Mentioned|Table 23|||||||||
27865|Nymerina Basalt|37460|3|Fully described|Table 3.I|||||||||
27865|Nymerina Basalt|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27865|Nymerina Basalt|39426|4|Described|p11|||||||||
27865|Nymerina Basalt|39444|4|Described|p33|||||||||
27865|Nymerina Basalt|39697|3|Fully described|p122|||||||||
27865|Nymerina Basalt|39837|6|Mentioned|Table 1|||||||||
27865|Nymerina Basalt|40369|6|Mentioned|p15|||See also Table 1||||||
27865|Nymerina Basalt|41357|6|Mentioned|Fig.2|||||||||
27865|Nymerina Basalt|41635|6|Mentioned|Table 2|||||||||
27865|Nymerina Basalt|41669|3|Fully described|p24|||||||||
27865|Nymerina Basalt|42352|5|Briefly described|p5|||||||||
27865|Nymerina Basalt|42785|5|Briefly described|Fig.3 P264|||||||||
27865|Nymerina Basalt|43055|4|Described|p15, Table 4|||of Fortescue Group||||||
27865|Nymerina Basalt|43056|5|Briefly described|Map Legend|||of Fortescue Group||||||
27865|Nymerina Basalt|43595|6|Mentioned|Table 2-29,p219|||Included within Pillingini Tuff (maybe superseded)||||||
27865|Nymerina Basalt|43698|6|Mentioned|p5|||||||||
27865|Nymerina Basalt|44152|6|Mentioned|p173, p176 Fig.2-154|||Originally Nymerina Basalt Member (of Mount Jope Volcanics) of MacLeod and de la Hunty (1966). Used with Formation status by Williams (1969). Obsolete; replaced by Maddina Formation.||||||
27865|Nymerina Basalt|44443|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group.||||||07-NOV-08
27865|Nymerina Basalt|46319|4|Described|p14|Proterozoic|Paleoproterozoic|Of Fortescue Group.  Maximum thickness: 300m.||||||07-NOV-08
27865|Nymerina Basalt|50189|5|Briefly described|p23|Archean|Archean|Name now discontinued. Formerly overlain by the Maddina Basalt - both reassigned as the Maddina Formation.||||||07-NOV-08
27865|Nymerina Basalt|50544|6|Mentioned|p44 Fig. 8|Archean|Archean|Of Hickman et al (1983).  Superseded by Maddina Formation of Williams (2003) - according to stratigraphic correlation chart for the Fortescue Group, YARRIE.||||||07-NOV-08
27865|Nymerina Basalt|60429|5|Briefly described|p20 Fig. 5, p21, p23|Archean|Archean|Name discontinued - rocks now included in Maddina Formation.||||||07-FEB-11
27865|Nymerina Basalt|60635|6|Mentioned|p51 Fig. 2.2A|||Now referred to as the Maddina Formation of Thorne and Hickman, 1998||||||
27865|Nymerina Basalt|61265|6|Mentioned|p48|||Geological Province: Pilbara Craton.||||||
27865|Nymerina Basalt|61575|5|Briefly described|p760 Fig. 2|||||||||
27865|Nymerina Basalt|61576|5|Briefly described|p774 Fig. 1|||Geological Province: Hamersley Basin.||||||
27865|Nymerina Basalt|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Geological province: northen Pilbara Craton.||||||07-FEB-11
27865|Nymerina Basalt|65825|6|Mentioned|p22.|Archean|Archean|Superseded name; now included in Maddina Formation.||||||
27865|Nymerina Basalt|65827|6|Mentioned|p33 Fig.6|Neoarchean|Neoarchean|In Nullagine 1:250 000 map. Subsequently included in Maddina Formation.
||||||
27865|Nymerina Basalt|65829|6|Mentioned|p15.|||Listed as occurring in the Nullagine 1:250 000 sheet (Hickman 1978); superseded, and the rocks included in the Maddina Formation.||||||
27865|Nymerina Basalt|67229|6|Mentioned|p3 Fig.2|||Of Hickman (1983), who divided the Pillingini Tuff of Kriewaldt and Ryan (1967) into three Formations including this unit.||||||
27865|Nymerina Basalt|69299|5|Briefly described|p4, p19|||Not current. Hickman (1983): mainly basalt, but including local units of tuff and rare rhyolite. Included within lower Maddina Basalt. This later renamed to Maddina Formation. Is sometimes shown as 'Nymerina Basalt' herein.||||||
27865|Nymerina Basalt|71808|6|Mentioned|p8|||Obsolete name superseded by the Maddina Formation.||||||
38080|Nymerina Basalt ""|23570|6|Mentioned|p165|||Informal - see Nymerina Basalt.||||||
40180|O'Callaghan Granite|24594|5|Briefly described|p608 Fig. 4|Neoproterozoic|Mesoproterozoic|Age: ~700-550Ma (Pb-Pb isochron, Geollnicht, 1992).  Geological Province: Paterson Orogen.||||||
74116|O'Callaghan's Granite|24197|5|Briefly described|p26|Neoproterozoic|Neoproterozoic|Of O'Callaghan's Supersuite. I-type (grandodioritic) Minyari type granite. Age: ~625Ma. Geological province: Paterson Province.||||||27-SEP-12
74100|O'Callaghan's Supersuite|24197|4|Described|p26|||Incl: Mt Crofton, Hansens Folly and Desert's Revenge Granites, ilmentite-bearing Mt Crofton-type; Koolyu, Minyari, O'Callaghan's Granites (Minyari-type). Geol. prov: Paterson Prov. See also O'Callaghans Supersuite (note spelling). Eg.of Cullen Assocn.||||||07-FEB-11
74166|O'Callaghans Suite|24197|5|Briefly described|p100|||One of two suites within O'Callaghans Supersuite - reduced; the other suite is Mount Crofton Suite (oxidised). See also reference to Supersuite p26, 27.||||||27-SEP-12
74166|O'Callaghans Suite|65454|5|Briefly described|p12|Cryogenian|Cryogenian|Of O'Callaghans Supersuite. Reduced and ilmenite-bearing, highly fractionated, I-type. Forms magnetic lows. Has a greater potential for gold than Mount Crofton Suite||||||
74166|O'Callaghans Suite|67202|4|Described|p55 Fig.3.4, p60, p190-191|||Wyborn (1997), Budd et al. (2001). Replaces the Minyari group of O'Callaghans Supersuite granites of Goellnicht et al. (1991).||O'Callaghans Supersuite.|Wilki, Minyari, Koolyu and O'Callaghans Granites.|Intrudes Lamil Group.|Granites.|
78630|Oak Hill Intrusion|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Gabbro; relict cumulate texture; metamorphosed.|06-AUG-15
78630|Oak Hill Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro; relict cumulate texture; metamorphosed.|
78630|Oak Hill Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro; relict cumulate texture; metamorphosed|
36853|Oak Hill Sill|23582|5|Briefly described|Map Legend|Archean|Archean|Gabbro, relict cumulate texture; metamorphosed.||||||07-NOV-08
25360|Oakover Beds""|39697|6|Mentioned|p9|||||||||
27216|Oakover beds|7433|5|Briefly described|pp48-50. |Tertiary|Late Cretaceous|Canning Basin. Intensively silicified. More extensive calcretes are up to tens of metres thick; local caves and other karst features developed.||||Overlies Precambrian rocks.|Calcrete.|
27216|Oakover beds|38878|6|Mentioned|Map legend|Pliocene|Miocene|Miocene - Pliocene||||||
27216|Oakover beds|44479|2|Defined|opp. p.7|||(beds). Lacustrine marl and limestone with chalcedonic capping, traces of ostracods.||||||
27216|Oakover beds|45153|2|Defined|App.11-162|late Pleistocene|late Pleistocene|Formerly Braeside Limestone.||||||
27216|Oakover beds|45158|3|Fully described|p12|||See also P34||||||
27216|Oakover beds|61155|5|Briefly described|p4, p16|Middle Miocene|Middle Miocene|Age: ~16-~12.5Ma. Thickness: 30m. Geological Province: Southern Canning Basin.||||||
30213|Ocellar basalt|43125|5|Briefly described|p5|||||||||03-MAR-10
42473|Olby Rock monzogranite|60708|6|Mentioned|p146 Fig. 7|||Informally named for the geographical locality of Olby Rock.||||||13-JAN-05
38610|Older Complex|23784|6|Mentioned|p42 Fig. 17|||Informal reference to the older granites of the Yule Granitoid Complex.||||||
32573|Older Greenstone Series|45473|14|Not recorded|p.80,84|||||||||
39190|Older"" Ascot Formation|23768|6|Mentioned|p57, p76, p181|||Geological Province: Perth Basin.  See also "older" Ascott Formation.||||||10-MAR-05
33757|Oldham Formation|64286|6|Mentioned|p75 Fig. 3|||Probably misspelt and should be Oldham Sandstone.||||||07-FEB-11
75192|Oliver Sand|65078|6|Mentioned|p35|||This is an example of a clastic "basal transgressive sand" - indicating deltaics and general shallow marine geology.  Geological province: Vulcan Sub-basin.||||||30-APR-09
28890|Oliver Sand Member|5952|5|Briefly described|p214 Fig. 4, p229|Miocene|Miocene|Pattillo and Nicholls (1990). In figure, Mbr = Member. Of Oliver Formation. Geological Province: Bonaparte Basin. Sandstones are predominantly quartzose, texturally sub-marine, and generally poorly sorted, grain-size very fine to very coarse||||||
28890|Oliver Sand Member|42053|5|Briefly described|Fig.17 P47|||||||||01-MAR-10
28890|Oliver Sand Member|62837|5|Briefly described|Stratigraphic columns|Oligocene|Oligocene|Of the Oliver Formation. Age: ~27-~25Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||08-NOV-06
28890|Oliver Sand Member|64697|5|Briefly described|p84 Fig.2 |Miocene|Miocene|||||||
34223|Oliver Sandstone|22663|5|Briefly described|AC97 1-4 Fig.4||Miocene|||||||
34223|Oliver Sandstone|23378|5|Briefly described|p180 Fig.2|Miocene|Oligocene|Also known as Oliver Sand Member, Oliver Formation. Of Woodbine Group, Vulcan Sub-basin.||||||01-MAR-10
34223|Oliver Sandstone|24218|6|Mentioned|p853 Fig. 5|||Misspelt - see Oliver Sandstone Member.   Geological Province: Bonaparte Basin.||||||
34223|Oliver Sandstone|61548|6|Mentioned|p480 Fig.3|Miocene|Oligocene|Northern Bonaparte Basin.||||||
34223|Oliver Sandstone|64689|6|Mentioned|p14|||May form a stratigraphic trap for Jurassic oil migrating up fault conduits.||||||
34223|Oliver Sandstone|68223|6|Mentioned|p178 Fig.3|Miocene|Oligocene|||||||
29407|Olympic Formation (WA)|41976|6|Mentioned|p453|||||||||
29407|Olympic Formation (WA)|41977|6|Mentioned|p471|||||||||
29407|Olympic Formation (WA)|43595|5|Briefly described|p350|||Of the Halls Creek Group. Mainly greywacke-siltstones with minor dolomite and felsic volcanic rocks.||||||
82118|One Gum Sandstone|72910|6|Mentioned|p22.|Artinskian|Artinskian|See also One Gum Formation. Abandoned name, now believed to be, in part, equivalent to the Ballythanna Sandstone Member.||||||
32947|One Gum limestone|48885|14|Not recorded|p.9||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6).||||||
32807|Onslow Beds|45038|14|Not recorded|p.16||Late Devonian|U.Dev.||||||
38724|Ooldea Sand, "lower"|24397|5|Briefly described|p240|||Informal subdivision of Ooldea Sand.  Interpreted as Ooldea Sand in the Ooldea Range.||||||
38722|Ooldea Sand, lower|24397|6|Mentioned|p237|||Informal - see Ooldea  Sand.||||||
72756|Ooldea sand|61814|5|Briefly described|p26|Eocene|Eocene|Informal name. Coastal barrier sands. Geological Province: Gawler Craton.||||||
38696|Opal Well Granite|23789|6|Mentioned|p30 Fig. 11|||||||||
29943|Opaline Well Complex|43821|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
29943|Opaline Well Complex|65415|5|Briefly described|p119 Fig.1, p121.|||May represent sub-volcanic equivalents to Louden Volcanics.||||Intrudes Cistern Formation and upper Mons Cupri Volcanics.|A suite of more mafic (including olivine and pyroxene cumulates), inequigranular, gabbroic and peridotitic rocks.|
37209|Opaline Well Granite|23784|5|Briefly described|p21 Fig. 8|Archean|Archean|Age: c.2765Ma.||||||07-NOV-08
37209|Opaline Well Granite|23793|5|Briefly described|p41|Archean|Archean|Age: c.2765Ma||||||07-NOV-08
37209|Opaline Well Granite|23936|5|Briefly described|p3, p12, Fig.4|Archean|Archean|Age: 2765 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
37209|Opaline Well Granite|24184|5|Briefly described|p717|Archean|Archean|Geological Province: Mallina Basin. Age: 2765 +/- 5Ma (Nelson 1997)||||||07-NOV-08
37209|Opaline Well Granite|24185|5|Briefly described|p750|Archean|Archean|Age: ca. 2765 Ma (Huston at al, 2002). Geological Province: Mallina Basin.||||||07-NOV-08
37209|Opaline Well Granite|24189|4|Described|p802 Fig.1, p803, p812|Archean|Archean|Age: ca. 2765 Ma. Geological Province: Mallina basin||||||07-NOV-08
37209|Opaline Well Granite|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 2765 Ma||||||07-NOV-08
37209|Opaline Well Granite|69299|6|Mentioned|p21|||Incorrect naming of Nerrely Leucogranite.||||||01-JUL-14
81883|Ora Banda Igneous Complex|70826|6|Mentioned|p8|Neoarchean|Neoarchean|eastern Yilgarn Craton.||||||
78631|Ora Banda Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 4 unnamed subunits.||Massive olivine cumulate (dunite) at base; bronzitite and norite; quartz gabbro and granophyre; late differentiate; gabbronorite; all metamorphosed.|06-AUG-15
78631|Ora Banda Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Massive olivine cumulate (dunite), bronzitite, norite, quartz gabbro, gabbronorite and granophyre; metamorphosed.|
78631|Ora Banda Intrusion|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv.|||||Massive olivine cumulate (dunite) at base; metamorphosed, bronzitite and norite; metamorphosed, quartz gabbro and granophyre; late differentiate; metamorphosed, gabbronorite; metamorphosed.|
72894|Ord River Tonalite suite|60724|5|Briefly described|p10|||Informal name. Of the Tickalara Metamorphics.||||||
82050|Ord River Tonalite''|72437|6|Mentioned|p10|||Previously of the Mabel Downs suite, now abandoned as it can be traced directly into the Mabel Downs Tonalite.||||||
78632|Orinda Intrusion|69152|5|Briefly described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Gabbro; metamorphosed.|07-AUG-15
78632|Orinda Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro; metamorphosed. Leucogabbro; coarse grained with granophyric texture; metamorphosed.|
78632|Orinda Intrusion|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv, 100k_geologyl10_lut.csv.|||||Gabbro; metamorphosed|
28896|Osborn Formation|42123|6|Mentioned|p26|||||||||
28896|Osborn Formation|42995|6|Mentioned|p26|||Misspelling of Osborne Formation?||||||
81864|Osborne Clay|68811|6|Mentioned|p180 tbl 39||Cretaceous|||||||
35875|Oscar Range complex|23338|6|Mentioned|915|||Devonian reef complexes.||||||17-OCT-12
79544|Osmond Group|69003|6|Mentioned|p5|||Halls Creek Orogen. Shown as Paleoproterozoic.||||||01-SEP-16
79544|Osmond Group|69597|6|Mentioned|p5 fig 2b|||||||||
79544|Osmond Group|70731|6|Mentioned|p268|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
34455|Osmond Range succession|22754|5|Briefly described|p7,  p11, Table3|Mesoproterozoic|Mesoproterozoic||||Helicopter Siltstone, Ahern Formation, Wade Creek Sandstone,Bungle Bungle Dolomite, Mount Parker Sandstone.|Correlated with Carr Boyd Group, Glidden Group.||
34455|Osmond Range succession|73255|6|Mentioned|p534|Mesoproterozoic|Mesoproterozoic|[Described as Mesoproterozoic in text, shown as Tonian in age on p534 Fig.2]|ca 1128 Ma||Mount Parker Sandstone, Bungle Bungle Dolomite, Wade Sandstone, Helicopter Siltstone.|Underlies the Duerdin Group and Fargoo Tillite.||
81309|Outcamp Bore Supersuite|70020|6|Mentioned|p122,132|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton. HFSE-enriched granitic supersuite. Occurs as a linear belt of foliated granitic rocks and dykes, internal to the greenstone sequences, ranging in composition from biotite monzogranite to tonalite (Champion and Cassidy, 2002).||||||
81309|Outcamp Bore Supersuite|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Eastern Goldfields Superterrane.|||||HFSE-enriched granites.|
81308|Outcamp Bore granite|70020|6|Mentioned|p122|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.|2710+\-6 Ma|||||
79884|Outcamp Tonalite|69181|6|Mentioned|p117|||Warrants further study for exploration for gold deposits [according to the author, as his results suggested this was a highly prospective formation with no known gold deposits on the basis of his analysis].||||||
77192|Outer Siltstone Formation|44139|6|Mentioned|p281, Table 3-15|Proterozoic|Proterozoic|Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation.| | ||||10-SEP-12
77193|Outer Siltstone Member|44139|6|Mentioned|p280, 281 table 3-15|||Of Telfer Formation. Informal name (of Turner 1983 PhD thesis). Also contains gold.| | ||||10-SEP-12
77177|Outer siltstone|23758|6|Mentioned|p9|||Informal mine sequence unit of the Telfer Member.||||||
83343|Owen monzogranite|68154|5|Briefly described|p164, 166, 168|||2km WSW of Mount Ellis.|2655 +/- 15 Ma.||||Light grey, foliated, seriate to rarely feldspar-porphyritic, medium-coarse-grained, biotite monzogranite.|
83343|Owen monzogranite|73391|5|Briefly described|Appendix p164, 166, 168.|||2km WSW of Mount Ellis.|2655 +/- 15 Ma.||||Light grey, foliated, seriate to rarely feldspar-porphyritic, medium-coarse-grained, biotite monzogranite.|
33978|Paarate Formation|22470|5|Briefly described|p13 Fig. 17|Campanian|Campanian|Of Sherbrook Group.||||||
81549|Padbury Group, Lower|71484|5|Briefly described|p125,135-137|||Geological province: Padbury Basin. Interpreted to have been deposited on the upper plate of the Yilgarn Craton subducting plate that was subducted beneath the already combined Glenburgh-Pilbara plate (Occhipinti et al., 2004).|||Includes Wilthorpe Formation and Labouchere Formation.|||30-AUG-19
81550|Padbury Group, Upper|71484|5|Briefly described|p125,138|||Geological province: Of Padbury Basin.||Unit of Padbury Group.|Shown as including Moorarie Supersuite, Millidie Creek Foramtion, Robinson Range Formation.|||30-AUG-19
41208|Padbury Group, lower|49896|3|Fully described|p6|Paleoproterozoic|Paleoproterozoic|Informal - see Padbury Group. Originally subdiv: into Peak Hill, Horseshoe Range, Labouchere and Robinson Range Beds (MacLeod 1970). Horseshoe Beds later excluded from group. Thickness: ~4000m||||||07-NOV-08
41208|Padbury Group, lower|50222|6|Mentioned|p327|||Informal - see Padbury Group.  Comprises Labouchere and Wilthorpe Formations.||||||
25374|Paddy Market Formation""|39697|6|Mentioned|p100|||See also Table 5.||||||
75097|Pakoota Sandstone|12891|5|Briefly described|p733 Fig. 2|Early Ordovician|Late Cambrian|Probably a misspelling of Pacoota Sandstone. Geological province: Amadeus Basin.||||||07-FEB-11
77233|Palgrave Group|67375|5|Briefly described|p20 Fig.11. |||Repeated use of an abbreviated form of Mount Palgrave Group.||||||
77233|Palgrave Group|69003|6|Mentioned|p37|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province.||||||
77233|Palgrave Group|72094|6|Mentioned|p12 Fig 9|Mesoproterozoic|Mesoproterozoic|[Probably a misspelling of Mount Palgrave Group]|||Includes Elisa Formation.|||
79553|Palgrave Volcanics|67128|6|Mentioned|p5 Fig.3|||Western Musgrave Province.||Bentley Supergroup.||||
35902|Palgrave volcanic association|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup.||||||15-DEC-08
35902|Palgrave volcanic association|44109|5|Briefly described|p117|||Informal name. Of the Bentley Supergroup. Mainly felsic volcanics.||||||
35902|Palgrave volcanic association|64580|4|Described|map legend||Mesoproterozoic|Of Bentley Supergroup. Rhyolitic volcanic and volcaniclastic rocks.||||||15-DEC-08
35902|Palgrave volcanic association|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Bentley Supergroup|||Rhyolitic volcanic and volcaniclastic rocks|
22620|Pandanus Monzogranite|72437|5|Briefly described|p86-87|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite monzogranite.|
83387|Panglo conglomerate|73391|5|Briefly described|p236, 241, 244, 247, 304, 306|||Boorara Domain. Shown as Panglo Conglomerate p236. Also Panglo conglomerate member p166-172.|2674 Ma.|||Unconformably overlies Government Dam member (Upper Black Flag Group). Correlative of Kurrawang Formation.||02-JUL-22
80212|Panglo member|71166|5|Briefly described|p23|||[An informal, probable company name from the Kanowna gold camp]|||||Polymictic conglomerate.|
80212|Panglo member|73391|5|Briefly described|vii, 132, 158, 160, 163, 166-172, 174|||See also p177, 182-183, 189, 192, 194, 196, 302, 333-336, 341, 348, 351, 417, 444. Kanowna district. Also presented as Panglo conglomerate member and Panglo conglomerate. Estimated true thickness of 3800m. A basal angular unconformity cuts all Boorara Domain units from Lower Basalt to uppermost Black Flag Group. Lithology detailed: stratigraphic column, photographs, photomicrographs. Tentatively placed in Kurrawang Formation for lack of geochronology.||Kurrawang Formation.||Overlies Grave Dam member/Grit and Golden Valley member unconformably. Correlative (tentative) of the Kurrawang Formation.|Remarkably undeformed. Polymictic conglomerate, sandstone, siltstone and carbonaceous shale; BIF and chert conglomerate unit higher in section.|
83940|Panglo sandstone|70482|6|Mentioned|p319|Archean|Archean|Part of greenstone successions around the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.||||Unconformably overlies the Kalgoorlie Sequence.|Continentally-derived sandstone and conglomerate.|
80099|Panhandle Dyke Suite|70826|6|Mentioned|p14 tbl 5|Orosirian|Orosirian|Hamersley region.|2008 Ma|||||
83883|Panorama Volcanic complex|69569|6|Mentioned|p288|||Pilbara Craton. Said to underlie the Strelley Pool Chert [suggesting confusion with Panorama Formation?] and yet have the same C isotope signature, and fractionations consistent with those in the Proterozoic biosphere, because of hydrothermal transport and redeposition.||||||
28905|Panorama sandstone|23955|6|Mentioned|p1256|||Informal name. Geological Province: Pilbara Craton||||||
28905|Panorama sandstone|41851|4|Described|p823|||||||||
37150|Pantapanta Formation|23758|4|Described|p8|Neoproterozoic|Neoproterozoic|Of Lamil Group. Geological Province: Yeneena Basin.||||||
81430|Panton Intrusion|70731|5|Briefly described|p270-272,274,277|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. [Also called Panton Intrusion on p270]. Emplaced within Tickalara Metamorphics c. 1856 Ma toward the end of the Hooper Orogeny (Page and Hoatson, 2000; Trudu and Hoatson, 2000).|c. 1856 Ma|||||
81430|Panton Intrusion|71873|5|Briefly described|p426,442-443|Orosirian|Orosirian|Geological province: Lamboo Province. Mafic-ultramafic intrusion, correlable to the Rose Bore Granite and coinciding with Paperbark Supersuite, Ruins Dolerite and Whitewater Volcanics, which reflects the suturing of the Western and Central zones during the amphibolite-granulite facies Hooper Orogeny.|1856 Ma|||||
81536|Panton Intrusions|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed layered mafic-ultramafic intrusions; dunite, wehrlite, Iherzolite, peridotite, melagabbro, norite, gabbronorite, gabbro, leucogabbro, anorthosite, ferrogabbro, and magnetite gabbro; minor chromitite layers.|
81536|Panton Intrusions|71113|6|Mentioned|p96|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. See Panton Suite.||||||
28906|Panton Shale|39210|5|Briefly described|Fig.18|||||||||
28906|Panton Shale|41840|6|Mentioned|p42|||Incorporated in the Panton Formation||||||
28906|Panton Shale|41864|6|Mentioned|p19|||Name superseded. This unit now part of the Panton Formation||||||
28906|Panton Shale|44965|14|Not recorded|Not recorded|||||||||
35388|Panton Sill|23205|6|Mentioned|p42|||Unknown State.||||||
35388|Panton Sill|64722|6|Mentioned|p22|||Informal name. Mafic-ultramafic intrusion. Of Halls Creek Orogen.||||||11-APR-12
31798|Panton intrusions|43854|5|Briefly described|Map Legend||Proterozoic|Variation on Panton complex?||||||
31798|Panton intrusions|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31798|Panton intrusions|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed layered mafic-ultramafic intrusions; dunite, wehrlite, Iherzolite, peridotite, melagabbro, norite, gabbronorite, gabbro, leucogabbro, anorthosite, ferrogabbro, and magnetite gabbro; minor chromitite layers.||||||
31798|Panton intrusions|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Replaced by Panton Suite? |||||Metamorphosed layered mafic-ultramafic intrusions; dunite, wehrlite, lherzolite, peridotite, melagabbro, norite, gabbronorite, gabbro, leucogabbro, anorthosite, ferrogabbro, and magnetite gabbro; minor chromitite layers.|04-AUG-15
31798|Panton intrusions|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Anorthosite, leucogabbro, leucogabbronorite, gabbro, melagabbro, ferrogabbro, magnetite gabbro, gabbronorite, norite, peridotite, dunite, wehrlite, lherzolite, harzburgite, chromitite layers; metamorphosed and foliated|
33974|Panton layered mafic-ultramafic intrusion|22547|5|Briefly described|p13|Orosirian|Orosirian|Age: 1856 +/- 2 Ma.||||||14-NOV-06
33974|Panton layered mafic-ultramafic intrusion|69747|6|Mentioned|p272|||Geological province: Halls Creek Orogen. ||||||
68815|Paperbark Suite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1860-1850Ma. Geological Province: Halls Creek Inlier.||||||07-NOV-08
68815|Paperbark Suite|67323|5|Briefly described|p29|||Emplacement of these plutons in the Lamboo Complex was synchronous with the high-T low-P Hooper Orogeny. Island arc setting or above a SE-dipping subduction zone.|~1870-1860 Ma.||||Granites.|
68815|Paperbark Suite|69420|6|Mentioned|p5:18|||Halls Creek Orogen. The Wagait Suite (Pine Creek Orogen) is probably an extension of this unit.||||||12-JUL-16
31883|Paperbark supersuite|22547|3|Fully described|p11||Orosirian|Within the Lamboo Complex, Halls Creek Orogen. Age: 1865- 1850 Ma. Previously "Bow River Granitoid Suite" (1988), previously "Bow River Granite" (1969)||||||14-NOV-06
31883|Paperbark supersuite|22716|5|Briefly described|p232|Orosirian|Orosirian|||||||
31883|Paperbark supersuite|22754|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|In the Lamboo Complex. Age 1865-1850 Ma||||||07-NOV-08
31883|Paperbark supersuite|23323|6|Mentioned|p456 Table 1|||Informal - see Paperbark Supersuite.||||||07-FEB-07
31883|Paperbark supersuite|23383|4|Described|p7-8|Paleoproterozoic|Paleoproterozoic|Elsewhere referred to as Paperbark Supersuite.  Age: c.1865-1850Ma.  Of the Bow River batholith.  Dominated by medium- to coarse-grained, I-type porphyritic biotite monzogranite and granodiorite.||||||07-NOV-08
31883|Paperbark supersuite|23599|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850 Ma.||||||07-NOV-08
31883|Paperbark supersuite|23751|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: 1865-1850 Ma.||||||07-NOV-08
31883|Paperbark supersuite|24173|6|Mentioned|p20, 27|Paleoproterozoic|Paleoproterozoic|Informal name. Of the Bow River Batholith. Age: 1865-1860Ma||||||07-NOV-08
31883|Paperbark supersuite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal name.  Age: 1865-1850Ma.  In the Bow River batholith (Hooper Orogeny).||||||07-NOV-08
31883|Paperbark supersuite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31883|Paperbark supersuite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|Informal||||||
31883|Paperbark supersuite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31883|Paperbark supersuite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Comprises eight granitoid units. Age: c.1865-1850Ma. In the Hooper Complex and Lamboo Complex western zone.||||||07-NOV-08
31883|Paperbark supersuite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31883|Paperbark supersuite|65409|4|Described|pp56-59. |Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen. Part of the Bow River batholith. Contains over 20 I-type granitoid plutons and subordinate coeval gabbro intrusions. Field relationships are described in some detail, concluding that granitoid and gabbroic magmas mingled extensively at high levels in the crust but did not mix and homogenize.|1865-1850 Ma.||||Medium- to coarse-grained, porphyritic, biotite-bearing monzogranite, syenogranite and granodiorite, with subordinate tonalite; local rapakivi granite; massive, fine- to medium-grained gabbro, with widespread biotite and quartz, little/no olivine.|20-FEB-17
31883|Paperbark supersuite|66845|4|Described|p535, p537 Fig.3, p538, p539, p540, p543|Paleoproterozoic|Paleoproterozoic|In Western zone of Lamboo Complex. No formal suites identified, but it is clear not all granites are petrographically, chemically and genetically related to each other, thus they cannot be considered to form a single suite. Closely related to Whitewater Volcanics and high-level porphyry intrusions (Gellatly et al. 1975; Griffin et al. 2000). Age U-Pb zircon SHRIMP ages of 1864-1852 Ma reported for coarse-grained granites in the Hooper Complex of King Leopold Orogen (Griffin et al. 2000). 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.|1865-1850 Ma; |Bow River batholith (Western Zone) and Hooper Complex|Neville Granodiorite, Paperbark Granite, Mount Nyulasy Granite||medium to coarse grained, porphyritic, I-type granodiorite, monzogranite, syenogranite and subordinate tonalite (Griffin et al. 2000); Coeval gabbro intrusions (biotite-bearing norite, gabbronorite, gabbro and diorite); high-K granites.|
31883|Paperbark supersuite|66846|4|Described|p547-549, p552-553, p556-p558|Orosirian|Orosirian|The oldest granites in the Lamboo Complex occuring in the Eastern Lamboo Complex and Hooper Complex. Together with the Sally Downs supersuite are part of the Bow River batholith. Age range probably from U-Pb SHRIMP dating of zircon (see p547). See also: p556 Fig.8.|1865-1850 Ma|Bow River batholith||||12-AUG-20
79274|Papunya Gabbro|68994|6|Mentioned|p23|||With Papunya ultramafic (intrusion), was emplaced into deep crust (>25 km) of Warumpi Province.|1637+/-2 Ma.|||||13-JAN-17
79274|Papunya Gabbro|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1637+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||gabbro.|
41166|Paradise Plains Formation|50302|5|Briefly described|Map Legend|Archean|Archean|Of the De Grey Group.  Includes: Salt Well Member. Overlies: Nimingarra Iron Formation.  Geological Province: Pilbara Craton.||||||07-NOV-08
41166|Paradise Plains Formation|50383|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
41166|Paradise Plains Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
41166|Paradise Plains Formation|61264|5|Briefly described|p62|||Of the De Grey Supergroup. Geological Province: East Pilbara Granite-Greenstone Terrane/Pilbara Craton.||||||20-AUG-07
41166|Paradise Plains Formation|63441|5|Briefly described|p6 Tb. 1|Archean|Archean|Formerly of De Grey Group in the Goldsworthy Basin. Redefined as Salt Well Member (of Bookingarra Formation in the Croydon Group).  Name is now obsolete.||||||30-MAR-16
41166|Paradise Plains Formation|63538|5|Briefly described|p8 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton. Basalt.||||||07-FEB-11
41166|Paradise Plains Formation|63854|6|Mentioned|p230|||||Of the De Grey Supergroup.||||
41166|Paradise Plains Formation|69167|6|Mentioned|178019.1.pdf|Archaean|Archaean|Age derived from samples of  sandstone (178019.1.pdf, 178020.1.pdf) and is the age of deposition of the sandstones.|3281 +/- 10 Ma - 3477 +/- 14 Ma (SHRIMP)|De Grey Group||||
41166|Paradise Plains Formation|69590|5|Briefly described|178019.1.pdf + other geochron files|||Geological province: Pilbara Craton. Of De Grey Superbasin. Sample GSWA 178019 (coarse sandstone) yielded an intepreted maximum depositional age of 3281+\-10 Ma for the sandstone (weighted mean 207Pb/206Pb). Sample GSWA 178020 (peble conglomerate) yielded an intepreted maximum depositional age of 3477+\-14 Ma for the conglomerate (weighted mean 207Pb/206Pb).||Unit of De Grey Supergroup.||||
41166|Paradise Plains Formation|70775|6|Mentioned|p59|||This name originally included the Salt Well Member before it was made obsolete by Van Kranendonk et al., 2006 when it was found to correlate with the Lalla Rookh Sandstone.||||||
31379|Parda Sandstone|43563|6|Mentioned|Fig.2,p5||Albian|Misspelling/variation of Parda Formation||||||
31379|Parda Sandstone|43656|6|Mentioned|Fig.2,p8|Aptian|Barremian|||||||
31379|Parda Sandstone|43746|6|Mentioned|Fig.2,p11|Aptian|Barremian|||||||
31396|Paringa Formation|22682|5|Briefly described|Fig9,p14||Archean|||||||07-NOV-08
31396|Paringa Formation|43629|5|Briefly described|p521|Archean||Misspelling/variation on Paringa Basalt. (late Archaean)||||||07-NOV-08
22629|Parker Range BIF|43295|3|Fully described|p5||Precambrian|Type,area,location given. Within a tholeiitic basalt unit.||||||
79229|Parkeston Dolerite|70153|5|Briefly described|100k_interpgeop_lut.csv|Proterozoic|Proterozoic||||||Quartz dolerite.|
79229|Parkeston Dolerite|71270|4|Described|100k_interpgeol_lut.csv|Proterozoic|Proterozoic|Events: Western Australian events (4000 - 0.01 Ma).|2500-541 Ma (inferred)|Unit of Lakewood Dolerite Suite.|||Quartz dolerite|
23893|Parmelia Formation|12758|5|Briefly described|p7, p18|||Previously mapped as part of the Yarragadee Formation; established as formation by Backhouse (1984).  Now superseded by Parmelia Group.  Geological Province: Vlaming Sub-basin.||||||22-JAN-07
23893|Parmelia Formation|12759|3|Fully described|p34; p28 Tb. 7; p32 Fig 15.|Berriasian|Tithonian|Defined Backhouse(1984). Type section in Peel No.1 Well (AMG Zone 50; 353561 m E, 6429303 m N; 1625-3551 m depth).|||Includes Carnac and Otorowiri Members.|Conformably overlies Yarragadee Formation; is overlain unconformably by Gage or Leederville Formations or South Perth Shale.|Interbedded sandstones, siltstones and shales.|12-MAY-14
23893|Parmelia Formation|23172|4|Described|Map Legend|Cretaceous|Late Jurassic|||||||
23893|Parmelia Formation|23279|4|Described|p8,29-30|Berriasian|Tithonian|(Backhouse, 1984).||||||
23893|Parmelia Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Late Jurassic|||||||
23893|Parmelia Formation|23761|4|Described|p6|||Formerly "South Perth Formation" and upper Yarragadee Formation.   Consists of a sequence of sand, siltstone and shale.  Max. thickness: >400m.   Geological Province: Dandaragan Trough.  See also p9.||||||
23893|Parmelia Formation|24160|6|Mentioned|p94|||Perth Basin.|||||Sandstone, siltstone, shale.|
23893|Parmelia Formation|24390|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
23893|Parmelia Formation|24410|6|Mentioned|p42|Jurassic|Jurassic|Found in the Dandaragan Trough. ||||||
23893|Parmelia Formation|40300|2|Defined|p2|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
23893|Parmelia Formation|40992|6|Mentioned|Fig.5|||||||||
23893|Parmelia Formation|41728|6|Mentioned|p441|||See also P443. Formerly Quinns Shale Member||||||
23893|Parmelia Formation|41989|4|Described|p111|||||||||
23893|Parmelia Formation|42194|5|Briefly described|p31|||||||||
23893|Parmelia Formation|42434|4|Described|p5|||||||||
23893|Parmelia Formation|42688|6|Mentioned|map legend|Cretaceous||||||||
23893|Parmelia Formation|42734|5|Briefly described|map legend|Cretaceous||||||||
23893|Parmelia Formation|43031|4|Described|p17,Fig.2.|||||||||
23893|Parmelia Formation|43096|5|Briefly described|p5|||see also Fig.2||||||
23893|Parmelia Formation|43216|5|Briefly described|Map Legend||Cretaceous|Perth Basin||||||
23893|Parmelia Formation|43217|5|Briefly described|Map Legend||Cretaceous|Perth Basin||||||
23893|Parmelia Formation|43296|5|Briefly described|Map Legend||Cretaceous|||||||
23893|Parmelia Formation|43297|5|Briefly described|Fig.3p5,p16.|Berriasian|Tithonian|see also table 1 p6.Type section location given.||||||
23893|Parmelia Formation|43347|6|Mentioned|5|||||||||
23893|Parmelia Formation|43495|4|Described|3-34|Berriasian|Tithonian|||||||
23893|Parmelia Formation|43504|4|Described|4-11|Neocomian|Tithonian|||||||
23893|Parmelia Formation|44144|4|Described|p505 Tb.4-21, p509 Fig.4-145, p514-515|Berriasian|Tithonian|Type Section: Peel 1 well: 1625-3551m.  8000m thick fluvial rocks.|||Includes Carnac and Otorowiri Members.|Overlies gradationally Yarragadee Formation. Is overlain unconformably by Dandaragan Sandstone and South Perth Shale.|Light grey to white, fine- to very coarse-grained sandstone, siltstone and grey shale.|
23893|Parmelia Formation|50085|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Age: <150Ma.  Geological Province: Northern Perth Basin.||||||11-MAY-04
23893|Parmelia Formation|61023|5|Briefly described|p20 Fig 10|Jurassic|Jurassic|Geological Province: Perth Basin.||||||11-APR-08
23893|Parmelia Formation|61811|6|Mentioned|p65.|Early Cretaceous|Late Jurassic|Raised to Group status by Crostella and Backhouse (2000). Type section details in Appendix 1.||||||
23893|Parmelia Formation|63017|5|Briefly described|p891, p892 Fig.1, p893|Early Cretaceous|Late Jurassic|Age: ~140Ma. Contains the Otorowiri Member (basal). Predominantly weathered feldspathic sst or sand interspersed with discontinuous lenses of clay and sltst. Fluvial in origin. Conformably overlies Yarragadee Fm. Max. thick: 500m. Geol Prov: Perth Basin||||||22-JAN-07
23893|Parmelia Formation|63018|5|Briefly described|p906, p907 Fig.1|Early Cretaceous|Late Jurassic|Outcrops on Dandaragan Plateau. Contains the Otorowiri Member. Overlies the Yarragadee Formation. Geological Province: Perth Basin.||||||
23893|Parmelia Formation|65306|6|Mentioned|p20 (2nd. figure)|||Conformably overlies the Yarragadee Formation and its aquifer.||||||10-SEP-09
23893|Parmelia Formation|67135|5|Briefly described|p5 Fig.7.|Jurassic|Jurassic|Perth Basin.||||Overlies Yarragadee Formation. Is overlain unconformably by South Perth Shale.||
23893|Parmelia Formation|67340|6|Mentioned|p7, 25, 50, 52, 60, 62|Cretaceous|Cretaceous|Onshore North Perth Basin (in Mory and Iasky, 1996). See also reference to Parmelia Group (p6). Wells in this unit used for this Report are listed.|||Otorowiri Member.|||
23893|Parmelia Formation|68135|5|Briefly described|p52 fig 2b |Early Cretaceous|Tithonian|Perth Basin.||||Overlies Yarragadee Formation.|Interbedded siltstone and sandstone.|14-SEP-17
23893|Parmelia Formation|68254|6|Mentioned|p1036 Fig.2, p1040, p1046 Tb.4|Cretaceous|Jurassic|||||||
41888|Parmelia Formation, Lower|12758|6|Mentioned|p47 Fig. 50|||Of Devereux (1993).  Probably same unit as the informal term "Lower Parmelia Sandstone"?  Preferred name now is Parmelia Group.||||||
41889|Parmelia Sandstone, Lower""|12758|6|Mentioned|p18, p46|||Informal reference to a sandstone unit between the Otorowiri and Carnac Members of the Parmelia Group, when the group was of formation status.  Now superseded by Jervoise Sandstone (Parmelia Group).||||||
83646|Parry Beach dyke|73480|5|Briefly described|p210, p216-218|Cambrian|Neoproterozoic|Likely associated with Kuunga Orogeny. Youngest zircon dates of 1183+/-10 Ma is likely inherited. See also Parry Beach basaltic dyke.|1183+/-10 Ma U-Pb zircon max. crystallisation age||||Basaltic andesite, unmetamorphosed.|
83355|Paterson Formation''|73117|6|Mentioned|p26|||[a variation on Paterson Formation written in inverted commas to denote particular usage].||||||31-AUG-22
83333|Paterson Range Series/Beds''|73117|6|Mentioned|p26|||Of Talbot (1920). [Superseded; see Paterson Formation]. [Written as 'Paterson Range Series/Beds'].||||||
31942|Paterson formation|43876|14|Not recorded|p573||Sakmarian|||||||
35675|Patterson Formation|23147|5|Briefly described|p139|||||||||
35675|Patterson Formation|23558|6|Mentioned|p33|||Misspelt. See Paterson Formation. Geological Province: Officer Basin.||||||
35675|Patterson Formation|68270|5|Briefly described|p678|Permian|Permian|Western Officer Basin. See reference to Paterson Formation (same unit)  p684.||||Underlain unconformably by Turkey Hill Formation.||13-JUL-21
31402|Peak Hill Formation|43238|5|Briefly described|p6|||Formerly Peak Hill Metamorphic Suite (Gee, 1979). Of Bryah Group.||||||
31402|Peak Hill Formation|61217|5|Briefly described|p42 Fig. 1|Proterozoic|Proterozoic|Of the Bryah Group. Metamorphosed sedimentary rocks - quartz, muscovite-schists.||||||07-FEB-11
31402|Peak Hill Formation|65419|5|Briefly described|p5, p30.|Paleoproterozoic|Paleoproterozoic|Originally the Peak Hill Beds of MacLeod (1970); subsequently Peak Hill Metamorphic Suite (Gee, 1979); Peak Hill Metamorphics (Gee, 1990); transferred to the Glengarry Group (Gee and Grey 1993); transferred to the Bryah Group and renamed as Peak Hill Formation (Pirajno and Occhipinti 1995); removed from Bryah Group (this study) as it is a tectonically bound unit with uncertain relationships with the Bryah Group.||||||
80541|Peak Hill Mylonite|70804|5|Briefly described|p5||||||||Refolded quartz blastomylonite and quartz mylonite lens with quartz-muscovite schist.|
68019|Peak Hill metamorphics|23798|6|Mentioned|p3|||Informal name. Geological Province: Yilgarn Craton.||||||05-JUL-06
41237|Peak Hill schist|50226|6|Mentioned|p422|||Informal - see Peak Hill Schist.||||||
81782|Pear Creek Intrusion|69185|5|Briefly described|GEOL_LUT_CSV files||Archean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||||||
77217|Pear Creek Sequence|60112|6|Mentioned|p109-110, p117. |||1.6 km of sedimentary rocks.||Unit in Fortescue Group.||||
77217|Pear Creek Sequence|66217|6|Mentioned|p48.|||Of Blake (1993); equivalent to Pear Creek Formation (p5, p6 Table 1, pp48-51).||||||
24452|Pearana Basalt|23570|4|Described|p238 App. 1|||Of Fortescue Group.   Overlain by Lewin Shale; underlain by Tumbiana Formation.   Thickness: ~500m.   Geological Province: Pilbara Craton||||||
24452|Pearana Basalt|23585|5|Briefly described|p14 Fig 5|Archean|Archean|Of Fortescue Group. Overlying unit Maddina Basalt. Underlying unit Kuruna Siltstone. Hamersley Basin.||||||07-NOV-08
24452|Pearana Basalt|23594|5|Briefly described|p9 Fig 6|Mesoproterozoic|Paleoproterozoic|Replaced by Maddina Basalt. Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
24452|Pearana Basalt|23745|5|Briefly described|p7 Fig 5|Proterozoic|Proterozoic|Replaced by Maddina Basalt.||||||
24452|Pearana Basalt|23746|5|Briefly described|p8 Fig 5|Proterozoic|Proterozoic|Renamed Maddina Basalt. Of Fortescue Group.||||||
24452|Pearana Basalt|36551|6|Mentioned|Table 23|||||||||
24452|Pearana Basalt|37460|3|Fully described|Table 3.I|||||||||
24452|Pearana Basalt|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24452|Pearana Basalt|39426|2|Defined|Table 1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24452|Pearana Basalt|39697|4|Described|p124|||||||||
24452|Pearana Basalt|42352|5|Briefly described|p5, Fig.3 p6, p17|||||||||
24452|Pearana Basalt|42785|5|Briefly described|Fig.3 P264|||||||||
24452|Pearana Basalt|43595|6|Mentioned|Table 2-29,p219|||Included in Maddina Basalt||||||
24452|Pearana Basalt|44152|5|Briefly described|p173, p176 Fig.2-154, p177|||Hickman (1978). Over 700m thick.||Mount Jope Volcanics|||Coarse-textured lower part; upper part characteristically vesicular, locally glomeroporphyritic;  andesitic and dacitic flows near top.|
24452|Pearana Basalt|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group. Isabella Range area.||||||07-NOV-08
24452|Pearana Basalt|46319|4|Described|p14|Mesoproterozoic|Paleoproterozoic|Of Fortescue Group.  Overlain by Tumbiana Formation.||||||07-NOV-08
24452|Pearana Basalt|50544|6|Mentioned|p44 Fig. 8|Archean|Archean|Now part of the Maddina Formation?||||||07-NOV-08
74048|Pearce Formation, Lower|13242|3|Fully described|p215,  p226 Fig. 8|Late Permian|Late Permian|Informal name but 'defined'. Comprises basal limestone of Pearce Fm - a possible definable unit lies between -Torrens Member, in the Petrel Sub-basin area. Overlies Fossil Head Fm abruptly; sharp transition with Upper Pearce Fme. Onshore this = sandstone.||||||07-FEB-11
74049|Pearce Formation, Upper|13242|3|Fully described|p215,  p226 Fig. 8|Late Permian|Late Permian|Informally named but 'defined'. Includes former Basal Member Member (Bhatia et el 1984) + Pearce Member (Mory 1988). Abrupt over Lower Pearce Fm; gradational below Cape Hay Fm. Dark grey, micaceous, slightly carbonaceous shale; bryozoan-rich calcarenites.||||||07-FEB-11
81846|Pearce Limestone|72505|5|Briefly described|p890|Wordian|Wordian|Southern Bonaparte Basin. Correlated to the Didecitriletes ericanus zone.||||Overlies the Torrens Formation. Overlain by the Cape Hay Formation.||
23895|Pearce Member|13194|4|Described|p387 Tb. 4-16, p405 fig 4-71|Permian|Permian|Type Section: Petrel 2 well (3952-3983m). 5-57m thick marine shelf deposits.||Hyland Bay Formation||Overlain by Cape Hay Member.|Biomicrite and biosparite limestone.|
23895|Pearce Member|13222|6|Mentioned|p229 Fig.2.|||Replaced by Pearce Formation.||Unit in Kinmore Group.||||
23895|Pearce Member|13234|6|Mentioned|p257. |Late Permian|Late Permian|||Unit in Hyland Bay Formation|||Reefal limestone.|
23895|Pearce Member|13242|5|Briefly described|p214 Fig. 2|Late Permian|Late Permian|Of Mory (1988). Of the Hyland Bay Formation (Kinmore Group); overlay unnamed base of the formation, underlay Cape Hay Member. Upgraded to Pearce Formation (Hyland Bay Sub-group) in this study. Geological Province: Bonaparte Basin.||||||07-FEB-11
23895|Pearce Member|41532|6|Mentioned|p301|||See also Fig.17||||||
23895|Pearce Member|42442|2|Defined|p19|Kazanian|Kungurian|Of Hyland Bay Formation.  Variation on Pearce Member, WA.||||||22-NOV-06
23895|Pearce Member|62837|5|Briefly described|Stratigraphic columns|Early Permian|Early Permian|Of the Hyland Bay Formation (Kinmore Group).  Age:  ~268-~264Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
23895|Pearce Member|69452|6|Mentioned|p36:20|||Defined by Mory (1988); raised to Formation status by Gorter (1998).||Hyland Bay Formation.||||12-JUL-16
23895|Pearce Member|71623|6|Mentioned|p354|Upper Permian|Upper Permian|Of McConachie et al (1996). Shown as 'Pearce and Dombey members'. Previously claimed to be reefs. That interpretation not accepted here. [presumably replaced by Pearce Formation of Hyland Bay Subgroup]||||||
25385|Pearce Member""|41532|5|Briefly described|p301|||||||||
80529|Pearce limestone, lower|71623|5|Briefly described|p358, p345 fig 2,  p347 fig 5||Roadian|Bonaparte Basin. Significant gas producer.|||||Limestone.|
80530|Pearce limestone, upper|71623|5|Briefly described|p358, p345 fig 2,  p347 fig 5||Roadian|Bonaparte Basin. Significant gas producer.|||||Limestone.|
38540|Peawah Granite|23813|5|Briefly described|p111|Archean|Archean|Age: 2950Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
38541|Peawah Granitoids|23813|6|Mentioned|p112|||Formal name not intended.  See also Peawah granitoids.  Geological Province: Pilbara Craton.||||||
38544|Peawah granitoids|23813|6|Mentioned|p90 Tb. 1|Archean|Archean|Informal - see also Peawah Granitoids.  Geological Province: Pilbara Craton.||||||07-NOV-08
38544|Peawah granitoids|23936|5|Briefly described|Tb.1|Archean|Archean|Age: >3.0-2.94 Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
34337|Pender Bay Conglomerate""|22718|6|Mentioned|P8||Cenozoic|||||||19-NOV-08
25388|Penneshaw Beds|29784|6|Mentioned|p19|||||||||
25388|Penneshaw Beds|30562|6|Mentioned|p8|||Refers Hall & Bekker (1965)||||||
25388|Penneshaw Beds|30900|4|Described|p68|||See also Table 1||||||
25388|Penneshaw Beds|31042|6|Mentioned|Fig. 4|||Correlation||||||
25388|Penneshaw Beds|34324|6|Mentioned|p126|||||||||
25388|Penneshaw Beds|37373|5|Briefly described|Table 2.I|||||||||
25388|Penneshaw Beds|41432|5|Briefly described|p13|||||||||
25388|Penneshaw Beds|42626|6|Mentioned|Fig.4 P10|||||||||
25388|Penneshaw Beds|45543|4|Described|p.101,102||Archean|||||||07-NOV-08
25388|Penneshaw Beds|73391|5|Briefly described|Appendices.|||Hall and Becker (1965). Regional stratigraphic correlation chart of other workers.|||||Greywacke and acid lithic tuff. ?Tholeiitic basalt.|
38649|Penneshaw Formation, Lower|23786|5|Briefly described|p5|Archean|Archean|Informal name.  Geological Province: Yilgarn Craton.||||||07-NOV-08
38649|Penneshaw Formation, Lower|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Norseman Terrane. The formally-named unit, Penneshaw Formation, has in this study been divided into lower (basalt) and upper (turbidites and BIF) parts. Part of the metavolcanic basement.|||||Tholeiitic and high MgO basalt.|
38649|Penneshaw Formation, Lower|66880|6|Mentioned|p8. |Archean|Archean|Superseded by Penneshaw Formation. Includes basalts.||||||
38649|Penneshaw Formation, Lower|70326|5|Briefly described|p360|Archean|Archean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton.||||Overlain by Upper Penneshaw Formation.|Basalt.|
38648|Penneshaw Formation, Upper|23786|5|Briefly described|p5|Archean|Archean|Informal name.  Geological Province: Yilgarn Craton.||||||07-NOV-08
38648|Penneshaw Formation, Upper|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Norseman Terrane. Kambalda Sequence. The formally-named unit, Penneshaw Formation, has in this study been divided into lower (basalt) and upper (turbidites and BIF) parts.|||||Thinly-bedded turbidites and BIF.|
38648|Penneshaw Formation, Upper|66880|6|Mentioned|pp7-8.|Archean|Archean|Superseded by Penneshaw Formation. Norseman Terrane.|c.2930 Ma (Campbell & Hill 1998).|||||
38648|Penneshaw Formation, Upper|70326|5|Briefly described|p360|Archean|Archean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton. Maximum depositional age from U-Pb SHRIMP detrital zircons (Nelson, 1995).|Max dep age: <2930+\-4 Ma (Nelson, 1995).|||Overlain by Noganyer Formation. Underlain by Lower Penneshaw Formation|Sediment, interflow sediment.|
38648|Penneshaw Formation, Upper|73391|6|Mentioned|Appendices.|||Krapez et al. (2000).|||||Internally differentiated felsic volcanic rocks, biotite rhyolite.|
30020|Penny Dam Conglomerate""|43075|5|Briefly described|p8|||||||||
30020|Penny Dam Conglomerate""|43593|5|Briefly described|p13|||||||||
77537|Penny Dam Sequence|66880|6|Mentioned|p10. |Archean|Archean|There is a formally-named unit, the Penny Dam Conglomerate. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank. Submarine-fan deposits.||||||
77565|Penny Dam Supersequence|66937|5|Briefly described|pp155-160.|Archean|Archean|Kalgoorlie Terrane. Confined to one fault-bound syncline. Upper greenschist facies. At least 2300 m exposed. Sandstones are classic turbidites; conglomerates are density-flow deposits.||||Unconformably overlies Kurnalpi and Minerie Sequences.|Lower succession of conglomerates, mostly clast-rich with rounded cobbles of basalt, felsic porphyry and granitoid; upper succession of sandstones, medium- to coarse-grained, graded; cappings of black shale and siltstone.|
77565|Penny Dam Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
32735|Penny Dam conglomerate|23584|6|Mentioned|p8|||||||||
32735|Penny Dam conglomerate|23786|5|Briefly described|p27|||Misspelt - see Penny Dam Conglomerate.  Geological Province: Yilgarn Craton.||||||
32735|Penny Dam conglomerate|24135|6|Mentioned|p41|||Informal name.||||||
32735|Penny Dam conglomerate|24174|5|Briefly described|p39|Archean|Archean|Informal name.  Geological Province: Eastern Goldfields.||||||07-NOV-08
32735|Penny Dam conglomerate|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
32735|Penny Dam conglomerate|60076|5|Briefly described|p12 Tb. 2, p14|||Probably an informal name.  Pebble to boulder clast-size;  quartzofeldspathic sandstone interlayers.  Max. thickness: 200m.  Geological Province: Gindalbie domain. (Yilgarn Craton).  See also p21.||||||13-APR-05
70327|Pentecost Sandstone, Lower|61571|6|Mentioned|p656 Fig. 3|||Informal - see Pentecost Sandstone.||||||
70326|Pentecost Sandstone, Middle|61571|6|Mentioned|p656 Fig. 3|||Informal - see Pentecost Sandstone.||||||
83814|Penzance granite|73631|5|Briefly described|p1-9|Archean|Archean|Yilgarn Craton. Associated with the Teutonic Bore VHMS Camp. SHRIMP U-Pb monazite age by Barrote et al. (2020). Is presented as Penzance Granite in p3 Fig.1C and p6 Fig.3.|2681.9 +/- 4.5 Ma.|Kent Complex.|||A relatively unweathered, HFSE-enriched granite.|
41126|Peperill Hill gneiss|24196|5|Briefly described|p68|Archean|Archean|Informal name. Age: 2678 +/- 7 Ma (SHRIMP U-Pb zircon: Black et al., 2002). Geological Province: West Agnew-Mount Clifford sub-domain.||||||07-NOV-08
83388|Perkolilli rhyolite|73391|5|Briefly described|p194, 196, 244, 246-247, 286, 304, 306|||Perkolilli rhyolite sequence of Taylor, 1984. See also p413, 419. Boorara Domain, Kalgoorlie Terrane. Often referred to as Perkolilli rhyolites. Hosts the Nimbus high-grade Ag-Hg deposit.|2675 +/- 3 Ma (Nelson, 1995).|Lower Black Flag Formation.||Overlies Talbot formation. Is overlain unconformably by Golden Valley member. Correlated with Lakewood dacite and Gibson-Honman formation.|High-SiO2 rhyolites.|02-JUL-22
75179|Peron sandstones|65027|6|Mentioned|p294|||Informal name.||||||16-APR-09
74689|Perserverance Supersuite|64580|4|Described|map legend||Devonian|Misspelling of Perseverence Supersuite. Undivided; granite.||||||15-DEC-08
74689|Perserverance Supersuite|69166|6|Mentioned|500k_geologyp08_lut.csv|Devonian|Devonian||||||Undivided; granite.|
38990|Perseverance Komatiite|23862|6|Mentioned|p30 Tb/ 1|||See also Perseverance Ultramafic Complex.||||||
73606|Perseverance Supersuite|63469|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|Consists of muscovite-tourmaline pegmatite; some rare-element bearing.||||||24-SEP-07
73606|Perseverance Supersuite|63470|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: 1030-950Ma. Leucocratic, medium-grained muscovite-tourmaline(-biotite) monzogranite; equigranular to porphyritic.||||||
73606|Perseverance Supersuite|65830|6|Mentioned|Plates 1,2|Neoproterozoic|Neoproterozoic|||||||
73606|Perseverance Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
38559|Perseverance dunite|24395|5|Briefly described|p212|||Informal name.||||||
28919|Perseverance gneiss|38512|6|Mentioned|Table III|||||||||
28919|Perseverance gneiss|38514|6|Mentioned|Fig.5|||||||||
38558|Perseverance komatiite|24395|6|Mentioned|p213|||Informal name.||||||
25391|Perseverance pegmatite""|38765|6|Mentioned|p102|||||||||
83879|Perseverance ultramafic sequence|69414|6|Mentioned|p101|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton.|<2711 +/- 2 Ma (age of footwall).|||||
83717|Perseverance ultramafic unit|70275|5|Briefly described|p485-487, 490, 492, 496, 498-499|||Perseverance Domain, Agnew-Wiluna Belt, Yilgarn Craton. Comprises four tectonic slices, extending over 21.5 km along strike. Also appears as Perseverance Ultramafic Unit.||||||
83717|Perseverance ultramafic unit|70276|6|Mentioned|p786 Fig.4|||Agnew-Wiluna greenstone belt, Yilgarn Craton. Appears as Mt Keith/Perseverance. Proximal extrusive facies. Hosts Ni-Cu-(PGE) mineralisation.|||||Lens dunites.|
34316|Perseverence Ultramafic Complex|22676|6|Mentioned|Fig23,p301|||||||||
38838|Pertataka limestone|24063|5|Briefly described|p219|Proterozoic|Proterozoic|Informal name.||||||
74799|Peter Piker Volcanics|64589|6|Mentioned|sample_locations file|||Misspelling of Peaker Piker Volcanics.||||||12-NOV-08
81312|Peter Well granodiorite|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton. See also Peter Well monzogranite, same page.||Unit of Eelya Suite.||||09-AUG-19
81313|Peter Well monzogranite|70020|5|Briefly described|p118,120|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton.||Unit of Eelya Suite.||||
40751|Petroglyph Orthogneiss|24554|4|Described|p8|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 3420 Ma (U-Pb). Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
40751|Petroglyph Orthogneiss|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Yule Granitoid Complex. Age: c. 3420 Ma. Geological Province: Pilbara Craton. Tonalitic orthogneiss with sheeted pegmatitic granitoid veins.||||||07-NOV-08
70640|Petroglyph orthogneiss|61252|6|Mentioned|p67 Tb.1|||Informal name. Of the Yule granitoid complex.||||||
28922|Petrol Formation Upper|42057|6|Mentioned|Fig.3 P70|||||||||
77220|Petter Calc Silicate|66299|6|Mentioned|p4 Fig.2.|Paleoproterozoic|Paleoproterozoic|Formal spelling is Petter Calc-silicate. Component of Glenburgh Terrane, basement to Gascoyne Province.||||||
77220|Petter Calc Silicate|73214|5|Briefly described|p974 Fig.1|Palaeoproterozoic||Glenburgh Terrane.||Camel Hill Metamorphics||||
80280|Phillipson beds|71080|6|Mentioned|p4|Neoproterozoic|Neoproterozoic|Of Wells (1962), Casey and Wells (1964). Now part of the Murraba Basin succession.||||||
25395|Pidinga Formation""|41517|6|Mentioned|p139|||||||||
38719|Pidinga Formation, lower|24397|5|Briefly described|p233|||Superseded by Maralinga Formation in South Australia, and by North Royal Formation in Western Australia.  Overlain by Paling Member.  Geological Province: Eucla Basin.||||||
38719|Pidinga Formation, lower|24606|4|Described|p958 Fig. 3|Middle Eocene|Middle Eocene|Informal - see Pidinga Formation. Overlain by the Paling Limestone. Geological Province: Eucla Basin. Formation is Fm in text.||||||
40776|Pig Well Conglomerate|24494|6|Mentioned|p14|||||||||
38661|Pig Well conglomerate|23786|5|Briefly described|p27|||Informal name.  Geological Province: Yilgarn Craton.||||||
36890|Pigeon Rock Monzogranite|23531|4|Described|p14.|Archean|Archean|Age: 2729+/-4 Ma (SHRIMP U-Pb zircon), see also page 7 fig.3. Yilgarn Craton Province.||||||07-NOV-08
36890|Pigeon Rock Monzogranite|65265|6|Mentioned|p75|||Suite has not been formally identified yet.||||||
36890|Pigeon Rock Monzogranite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, West Australian Craton. Events: Youanmi Terrane events (3200-2600 Ma).|2729+\-4 Ma||||Biotite monzogranite; equigranular; metamorphosed|
36890|Pigeon Rock Monzogranite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Youanmi Terrane, Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2729+/-4 Ma||||Biotite monzogranite; equigranular; metamorphosed.|
37931|Pigeon Rocks Granodiorite|24306|5|Briefly described|p936 Fig. 1|||Geological Province: Yilgarn Craton||||||
81397|Pigs head porphyry''|67553|5|Briefly described|p21|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Similar in composition to Wururu Rhyolite, and coeval with high-level block-faulting (caldera subsidence) and emplaced at 1065-1063 Ma along faults.|1065-1053 Ma||||Porphyritic microgranite.|
80025|Pilara Sequence|69297|6|Mentioned|p337, p352|Famennian|Frasnian|Canning Basin. Same mistake on two diagrams.||||Unconformably overlain by the Laurel Formation.||20-SEP-17
40338|Pilbara Craton Granitoids|24573|6|Mentioned|p670 Fig.1|||Not intended as a formal name. Geological Province: Pilbara Craton||||||
25396|Pilbara Group|39867|6|Mentioned|p21|||||||||
25396|Pilbara Group|43698|6|Mentioned|p3|||||||||
73586|Pilbara high-Mg diorite suite""|63441|6|Mentioned|p37|Archean|Archean|Informal reference to the Indee Suite (Sisters Supersuite).||||||07-FEB-11
33905|Pilga Station leucoadamellite|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2943 Ma||||||07-NOV-08
40166|Pilgangoora basalts|24621|5|Briefly described|p85|||Informal reference to the basalts of the Warrawoona Group in the Pilgangoora Belt.||||||
35874|Pillara Complex|23338|6|Mentioned|915|||||||||
28925|Pillara Limestone""|24000|5|Briefly described|p347|||Informal name.||||||
28925|Pillara Limestone""|40837|6|Mentioned|p264|||||||||
28925|Pillara Limestone""|41023|6|Mentioned|p289|||||||||
28925|Pillara Limestone""|45133|6|Mentioned|Fig.8|||||||||
28925|Pillara Limestone""|45143|3|Fully described|Fig.3|||Time-stratigraphic interpretations.||||||
28267|Pillara Range Granodiorite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Variation of Pillara ?||||||07-NOV-08
28267|Pillara Range Granodiorite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex|||Coarse-grained biotite granodiorite, minor medium-grained biotite tonalite.|
79143|Pillara Reef Complex|13255|6|Mentioned|p368|Late Devonian|Late Devonian|Oobagooma Sub-basin, Roebuck Basin.||||Overlies Tandalgoo and Poulton Formations. Is overlain by Laurel Formation.||
31914|Pillard formation|43876|14|Not recorded|p561||Givetian|||||||
69910|Pimbyana Granite""|61262|6|Mentioned|p459 App.|||Informal - see Pimbyana Granite. A synonym introduced by Krapez (1999) but not adopted. ||||||
33923|Pimbyana Granitoid|22484|6|Mentioned|p74|Statherian|Orosirian|||||||
33923|Pimbyana Granitoid|66299|6|Mentioned|p258.|||A term introduced by Krapez (1999) for the Pimbyana Granite of Pearson et al. (1996); no justification was advanced for the name change, which has not been formalised.||||||
69911|Pimbyana Granitoid""|61262|6|Mentioned|p459 App.|||Informal - see Pimbyana Granite.||||||
73621|Pinbyana Granite|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Misspelt - place name is Pimbyana.Of the DurlacherSupersuite. Age: 1680-1620Ma. Geological Province: Gascoyne Complex. Massive, medium-grained, megacrystic and porphyritic biotite(-muscovite) monzogranite; tabular megacrysts of K-feldspar up to 7cm long.||||||07-NOV-08
28207|Pincunah Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2. Reserved as Pincunnah Adamellite.||||||07-NOV-08
28207|Pincunah Adamellite|39697|3|Fully described|p38|||||||||
28207|Pincunah Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||165 sq. km. Post-tectonic granitoid.||Yule Granitoid Complex||Intrudes Warrawoona Group greenstones.|Porphyritic biotite monzogranite; granodiorite; tonalite, foliated.|
77797|Pincunah Banded Iron Member|68282|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Age inferred from parent unit.|3252-3235 Ma (Buick et al. 2002).|Of the Kangaroo Caves Formation|||Banded iron-formation; jaspilitic; minor layered chert and shale; metamorphosed.|
75916|Pincunah Banded-iron Member|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Member of Kangaroo Caves Formation. Banded-iron formation; jaspilitic; minor layered chert and shale; metamorphosed.||||||
75916|Pincunah Banded-iron Member|66745|5|Briefly described|p54 Fig.4.|||||Unit in Kangaroo Caves Formation.|||Banded iron-formation, chert.|
75916|Pincunah Banded-iron Member|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Kangaroo Caves Formation.|||BIF.|
75916|Pincunah Banded-iron Member|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Kangaroo Caves Formation.||||
75916|Pincunah Banded-iron Member|68035|5|Briefly described|p288 Fig 4|Paleoarchean|Paleoarchean|Sulphur Springs Group, Pilbara Supergroup, East Pilbara Terrane, Pilbara Craton. ||Top of Kangaroo Caves Formation|||Banded iron formation.|
75916|Pincunah Banded-iron Member|68280|5|Briefly described|p4|||||Kangaroo Caves Formation|||Banded iron formation and chert.|
75916|Pincunah Banded-iron Member|68284|6|Mentioned|p7|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Kangaroo Caves Formation.||||
75916|Pincunah Banded-iron Member|69301|5|Briefly described|p5 Fig.3|||Pilbara Craton. East Pilbara Terrane.||Kangaroo Caves Formation|||Banded-iron formation.|
75916|Pincunah Banded-iron Member|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||banded iron formation|
32216|Pincunah Hill Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Soanesville Subgroup, Pilbara Craton||||||07-NOV-08
32216|Pincunah Hill Formation|23755|4|Described|p42|Archean|Archean|See also page 17 table 1. Of Gorge Creek Group.||||||07-NOV-08
32216|Pincunah Hill Formation|23783|5|Briefly described|p10 Fig. 5|Archean|Archean|Of Gorge Creek Group.||||||07-NOV-08
32216|Pincunah Hill 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: 1200m.  Geological Province: Pilbara Craton.||||||07-NOV-08
32216|Pincunah Hill Formation|24184|6|Mentioned|p699 Fig.3|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
32216|Pincunah Hill Formation|24531|4|Described|p20|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). Conformably overlain by Corboy Formation. Geological Province: Pilbara Craton.  See also p5 Tb. 1.||||||07-NOV-08
32216|Pincunah Hill Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of Soanesville Subgroup (Gorge Creek Group).  Age: <3240Ma.||||||07-NOV-08
32216|Pincunah Hill Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Gorge Creek Group. Shale, BIF, sandstone, felsic volcanics. Age: <3235Ma.  Max. thickness: 3.5km. Geological Province: Pilbara Craton.||||||07-FEB-11
32216|Pincunah Hill Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). Sandstone, mudstone, minor comglomerate Fe-shale, BIF, interbedded sandstone, felsic volcanic rocks.||||||07-FEB-11
32216|Pincunah Hill Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
32216|Pincunah Hill Formation|61266|4|Described|p58 Tb.1, p60|Archean|Archean|Of the Soanesville Subgroup (Gorge Creek Group). In places conformably overlain by Corboy Formation. Fe-shale, BIF, interbedded sandstone, felsic volcanic rocks. Max. thickness: ~1200m. Geological Province: Pilbara Craton.||||||07-NOV-08
32216|Pincunah Hill Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Gorge Creek Group||||||07-NOV-08
32216|Pincunah Hill Formation|63441|4|Described|p4 Tb. 1, p6 Tb. 1, p22|Archean|Archean|Formerly of Gorge Creek Gp. Now redefined as Pincunah Member. Originally defined as a lower BIF unit+upper shale unit, the BIF is now interpreted to be a member of Kangaroo Caves Fm (Sulphur Springs Gp). The shale component is now named Cardinal Formation||||||07-FEB-11
32216|Pincunah Hill Formation|63538|4|Described|p6 Fig. 3|Archean|Archean|Of Soanesville Group. Underlain by Budjan Creek Formation. Geological Province: Pilbara Craton. Felsic volcanic rocks.||||||19-APR-13
32216|Pincunah Hill Formation|64328|5|Briefly described|p56 Tb. 1|||Of the Soanesville Subgroup (Gorge Creek Group). Shale, banded iron formation.||||||07-FEB-11
32216|Pincunah Hill Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Gorge Creek. Geological Province: Pilbara Craton. Banded iron-formation; red and black layered; thinly to moderatly bedded; weakly metamorphosed.||||||
32216|Pincunah Hill Formation|66118|5|Briefly described|p149 Fig.3|||Pilbara Craton. East Pilbara Terrane. ||||Dalton Suite intrudes Pincunah Hill Formation in Soanesville greenstone belt. Is overlain by Corboy Formation.||
32216|Pincunah Hill Formation|72668|6|Mentioned|p4|||East Pilbara Terrane.||Soanesville Group||Overlain by the Corboy Formation.||13-JAN-22
81783|Pincunah Hill Iron 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.||||
70158|Pincunah Member|63441|2|Defined|p4 Tb. 1|Archean|Archean|Supersedes Pincunah Hill Formation. Of Kangaroo Caves Formation (Sulphur Springs Group, Pilbara Supergroup). Consists mainly of BIF.||||||07-FEB-11
70158|Pincunah Member|67130|5|Briefly described|p16|||||Kangaroo Caves Formation|||Banded iron formation.|
70158|Pincunah Member|72668|5|Briefly described|p6|||Of Van Kranendonk et al. (2006). East Pilbara Terrane. <500m thick.||Kangaroo Caves Formation, Sulphur Springs Group.|||Banded-iron formation.|13-JAN-22
80300|Pincunah banded iron member|71041|6|Mentioned|p43|||Deep hydrothermal setting for deposition.||Of Kangaroo Caves Formation.||||
24456|Pincunnah Adamellite|39697|6|Mentioned|Fig.31|||Misspelling of Pincunah?||||||
80752|Pindan sand|71892|6|Mentioned|p18-p19|||Informally named dunal deposit.|||||Fine- to coarse-grained, rounded and frosted quartz sand dunes characterised by deep-red colour and moderate to high clay content.|28-FEB-19
75913|Pindan soil|65553|5|Briefly described|p1-2, p5 Fig.5, p6||Pleistocene|Less that 2 Ma. Around James Prices Point. Eolian and alluvial, up to 10 m thick. Also referred to as 'Pindan soil'.||||Overlies Broome Sandstone.|Red sandstone and siltstone including cemented eolian carbonate sandstone (relict coastal sand dunes).|30-MAR-12
25398|Pindar Beds|29813|4|Described|Table 2|||||||||
25398|Pindar Beds|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25398|Pindar Beds|45140|2|Defined|p13,p40, p42-43, p51, p66, p74, Appx.p22|||Blake et al. (1977). Named after Pindar Yard, beside Jawinga Pool on Sturt Creek. Birrindudu Basin. Mapped as Gardiner Beds and Kearney Beds by Casey and Wells (1964). Exposed as low strike ridges and as rubble on sandy plains. 300m thick. Beds dip steeply and are overturned. The reference area is 2km SW of the northern Palm Springs in the Denison Range, at 19deg 16'S, 128deg 17'E.||||Conformably overlies Lake Willson Beds. Tentatively correlated with Coomarie Sandstone. Is inferred to be overlain unconformably by Denison Beds and Chuall Beds.|Cross-bedded, medium- to coarse-grained quartz arenite and sublithic arenite; locally bedding planes are crowded with shale pellets.|
25398|Pindar Beds|46864|6|Mentioned|p38|||||||||
76003|Pindiliya Formation|66579|5|Briefly described|Map legend|Neogene|Neogene|Southern Carnarvon Basin. Age: ?Miocene.|||||Poorly sorted sandstone, commonly lithic, and granule to pebble conglomerate; generally very silicified.|19-SEP-13
38140|Pindilya Group|23569|4|Described|p8|Tertiary|Tertiary|Geological Province: Carnarvon Basin||||||
32948|Pindilya formation|48885|14|Not recorded|p.2||Tertiary|(G/50-6).||||||
41127|Pindinnis granite|24196|5|Briefly described|p46|Archean|Archean|Age: 2664 +/- 5 Ma (Fletcher et al., 2001)||||||07-NOV-08
41127|Pindinnis granite|67198|5|Briefly described|p51|||Laverton area.|2667 +/- 4 Ma.||||High-Ca granite.|
70709|Pindyin Beds""|62453|6|Mentioned|p17|||Informal name.||||||
77408|Pindyin Formation|65416|6|Mentioned|p137.|Neoproterozoic|Neoproterozoic|Officer Basin. Part of Sequence LP1A of Supersequence PL1.||||||
75799|Pingandy supersequence|24607|5|Briefly described|p968|||Prograding submarine fan part of the Ashburton Formation. Also includes the Mount Boggola volcanic succession in SE.||||||
29408|Pininnya beds|42940|5|Briefly described|Plate 2, Plate 3|Neoproterozoic|Neoproterozoic|Misspelling of Pinyinna beds.  Dolostone, limestone, siltstone, chlorite and talc schist.  Geological province: Amadeus Basin.||||||23-JAN-08
32640|Pinjian Breccia|23745|5|Briefly described|p7 Fig 5|Proterozoic|Proterozoic|Replaced by Pinjian Chert Breccia.||||||
32640|Pinjian Breccia|44443|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
32640|Pinjian Breccia|46319|2|Defined|p33 App. 1|Mesoproterozoic|Paleoproterozoic|Replaces Pinjian Chert Breccia and "Pinjian Chert Breccia".  Overlain by Carawine Dolomite; underlain by Waltha Woora Formation.  Maximum thickness: 100m.  Geological Province: Pilbara Craton.||||||07-NOV-08
38776|Pinjian Chert|23890|5|Briefly described|p5 Fig.2|||||||||
38568|Pinjian Chert Breccia""|46319|6|Mentioned|p33 App. 1|||Informal name - see by Pinjian Breccia.||||||
41866|Pinjin Chert Breccia|50544|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic|Misspelt - see Pinjian Chert Breccia.||||||07-NOV-08
78633|Pinjin Dyke|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Mainly dolerite and gabbro; includes cumulate and granophyric differentiates.|07-AUG-15
78633|Pinjin Dyke|70153|5|Briefly described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|||Widgiemooltha Dyke Suite|||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
78633|Pinjin Dyke|71270|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Yilgarn Craton, West Australian Craton.||Unit of Widgiemooltha Dyke Suite.|||Mainly dolerite and gabbro; includes cumulate and granophyric differentiates|
34398|Pinnyinna beds|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
25401|Pinyinna Beds|22803|6|Mentioned|p423|||||||||
25401|Pinyinna Beds|22805|5|Briefly described|p464|||Bitter Springs equivalent.||||||
25401|Pinyinna Beds|22826|6|Mentioned|p567|Neoproterozoic|Neoproterozoic|||||||
25401|Pinyinna Beds|24301|5|Briefly described|p15, p7 Tb. 2|||Pinyinna beds is probably the correct name.  Geological Province: Amadeus Basin||||||
25401|Pinyinna Beds|30815|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25401|Pinyinna Beds|30817|5|Briefly described|p9|||See also p14. Correlated with Bitter Springs Formation||||||23-NOV-06
25401|Pinyinna Beds|33588|4|Described|Table 2|||See aslo p6.||||||23-NOV-06
25401|Pinyinna Beds|33596|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25401|Pinyinna Beds|34442|6|Mentioned|p7|||Proterozoic. Correlates with Bitter Springs Formation.||||||23-NOV-06
25401|Pinyinna Beds|35102|6|Mentioned|p1|||||||||
25401|Pinyinna Beds|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25401|Pinyinna Beds|36887|5|Briefly described|p208|||||||||
25401|Pinyinna Beds|38157|6|Mentioned|Table VI|||||||||
25401|Pinyinna Beds|39210|5|Briefly described|p34|||See also Fig.10||||||
25401|Pinyinna Beds|39565|6|Mentioned|p33|||||||||
25401|Pinyinna Beds|40740|6|Mentioned|p1|||||||||
25401|Pinyinna Beds|41190|6|Mentioned|Fig.4|||||||||
25401|Pinyinna Beds|41270|6|Mentioned|Table 1|||||||||
25401|Pinyinna Beds|41717|6|Mentioned|Fig.2|||||||||
25401|Pinyinna Beds|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
25401|Pinyinna Beds|41852|6|Mentioned|Table 1|||||||||
25401|Pinyinna Beds|42082|6|Mentioned|Fig.3 P323|||||||||
25401|Pinyinna Beds|42504|6|Mentioned|p76|||||||||
25401|Pinyinna Beds|42940|5|Briefly described|Plate 9|||||||||
25401|Pinyinna Beds|44342|6|Mentioned|p.5|||SG/53-5.||||||
25401|Pinyinna Beds|44493|4|Described|p.10, map|||Correlates with Bitter Srpings Formation. BLOODS RANGE sheet. (G53-3). See p.9,12, for details.||||||23-NOV-06
25401|Pinyinna Beds|44494|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
25401|Pinyinna Beds|44495|4|Described|p.5, map||Neoproterozoic|AYERS ROCK sheet (G52-8). Upper Proterozoic. See p.7,9, for details.||||||23-NOV-06
25401|Pinyinna Beds|44496|5|Briefly described|map legend||Neoproterozoic|Grey phyllite, quartz-sericite schist, amphibole schist, Upper Proterozoic.||||||02-DEC-04
25401|Pinyinna Beds|44499|14|Not recorded|opp.p.6, Tb.1||Proterozoic|||||||
25401|Pinyinna Beds|45041|4|Described|p25|||See also p20 and Fig.7||||||23-NOV-06
25401|Pinyinna Beds|45085|6|Mentioned|p14|||Structure discussed.||||||
25401|Pinyinna Beds|45149|2|Defined|p26|Neoproterozoic|Neoproterozoic|See also Table 1.||||||
25401|Pinyinna Beds|48864|2|Defined|p.24,25||Neoproterozoic|Tb.1. On many pages. p.1,9,10,23,28,29,37,44,46,47,49,50,Pl.10,11,13,5,8,12. U.Proterozoic (G52-3,7,8).||||||
25401|Pinyinna Beds|48865|14|Not recorded|Pl.9|||(Ayers Rock Prelim.1:250,000). (G52-8).||||||
25401|Pinyinna Beds|48963|6|Mentioned|Fig.3|||See also Plate 5.||||||
25401|Pinyinna Beds|62359|5|Briefly described|p547, p548 Fig. 8|||Overlie Dean Quartzite. Thickness locally: >2km. Geological Province: Amadeus Basin. Equivalent to Bitter Springs Formation. Succession of metacarbonates, siltstones, and local evaporites. ||||||
25401|Pinyinna Beds|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Dolomite, limestone, siltstone. Metamorphosed in part to chlorite and talc schist. Underlies Inindia Beds. Overlies: Dean Quartzite.||||||14-AUG-06
25401|Pinyinna Beds|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Dolomite, limestone, siltstone. Metamorphosed in part to chlorite and talc schist.||||||
25401|Pinyinna Beds|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
25401|Pinyinna Beds|70018|4|Described|p234-240|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the southern Amadeus Basin. Correlable to Bitter Springs Formation in the northern Amadeus Basin. Deposition occurred during post-rift subsidence after initial uplift of Musgrave Block in a braod intracratonic basin between Musgrave Block and Arunta region. Thickness: up to 200m. Gradationaly contact with the overying Dean Quartzite, with ~1m of interlayered phyllite and quartzite (Scrimgeour et al., 1999). Undergone low- to moderate-grade metamorphism during ?550 Ma Petermann Orogeny. U-Pb dates on zircons this study and Close et al., 2003 show a broad peak from ?1060 Ma to 1170 Ma, suggesting a dominant zircon provenance from Musgrave Block, and severely diminished input from Arunta region.||||Overlain unconformably by Inindia Beds. Underlain by Dean Quartzite.|Grey, brown and white laminated micaceous siltstone overlain by grey and pink, laminated, variably stromatolitic, grey dolostone. Metamorphosed sediments include grey to purple-grey phyllites, thinly laminated with strong, usually crenulated fabric.|
25401|Pinyinna Beds|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
77397|Pinyinna Formation|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
23909|Pipeline Andesite Member|22534|4|Described|p21, Fig.4 p7|Archean|Archean|of Black Flag Group||||||07-NOV-08
23909|Pipeline Andesite Member|42382|6|Mentioned|Table 1 P9|||See also Pipeline Andesite.||||||
23909|Pipeline Andesite Member|43074|6|Mentioned|Table 1|||||||||
41088|Pipeline andesite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Ora Banda Domain.  Of the Black Flag Beds.  Age: 2681 +/- 5Ma.||||||07-NOV-08
74714|Pippingarra Granitic Complex|64580|4|Described|map legend||Mesoarchean|Undivided granitic rocks; metamorphosed.||||||15-DEC-08
74714|Pippingarra Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
35250|Pippingarra Granitoid Complex|23780|5|Briefly described|p114|Archean|Archean|Age: ~2928+/-6 Ma.||||||07-NOV-08
35250|Pippingarra Granitoid Complex|23783|5|Briefly described|p18|Archean|Archean|||||||07-NOV-08
35250|Pippingarra Granitoid Complex|23794|5|Briefly described|Map Legend|||||||||
35250|Pippingarra Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 2955-2928Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
35250|Pippingarra Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
35250|Pippingarra Granitoid Complex|24166|4|Described|p14|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
35250|Pippingarra Granitoid Complex|24184|4|Described|p703|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.2935Ma||||||07-NOV-08
35250|Pippingarra Granitoid Complex|24327|5|Briefly described|Map Legend|Archean|Archean|Age: 2955-2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35250|Pippingarra Granitoid Complex|24349|5|Briefly described|Map legend|Archean|Archean|Age: c.2995-2940Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
35250|Pippingarra Granitoid Complex|50302|5|Briefly described|Map Legend|Archean|Archean|Includes the Chillerina Granodiorite.  Geological Province: Pilbara Craton.||||||07-NOV-08
35250|Pippingarra Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as 2955-2850 Ma; also of Kenny (2000).|2941+/-4, 2954+/-4 Ma (Nelson 2000)||||undivided biotite(-hornblende), and hornblende(-biotite)-bearing diorite to monzogranite, and biotite(-muscovite)-bearing granite; metamorphosed|
39766|Pippingarra granitoid complex|24193|5|Briefly described|p874 Fig.1, p889|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
39767|Pippingarra pegmatite|24193|5|Briefly described|p873, p882|Archean|Archean|Not intended as a formal name. Geological Province: Pilbara Craton.||||||07-NOV-08
39251|Pirie Calcarenite Member|24094|5|Briefly described|p275|||Name used interchangably with Pirie Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
70566|Pitjantjatjara Suite|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Misspelt? - should be Pitjantjatjara Supersuite. Deformed granite. Geological Province: Musgrave Province.||||||
70566|Pitjantjatjara Suite|61864|6|Mentioned|p18 fig 4|||[Database says this is replaced by P. Supersuite]|||||Deformed granite.|
70566|Pitjantjatjara Suite|64745|6|Mentioned|p380 Fig.5|||Probable misspelling. See Pitjantjatjara Supersuite.||||||
76750|Pitjantjatjarra Supersuite|65693|6|Mentioned|p4, p12.|||Mis-spelling of Pitjantjatjara.|1149 Ma.|||||22-APR-20
76750|Pitjantjatjarra Supersuite|65898|5|Briefly described|Map legend|||Mis-spelling of Pitjantjatjara Supersuite||||||
29993|Plantagenent Group|43065|5|Briefly described|Fig.5,p92|Late Eocene|Middle Eocene|Misspelling of Plantagenet Group?||||||
69384|Plover Bore komatiite|60979|5|Briefly described|p86 Fig.2, p90, p92|||Informal name. Part of the Jundee sequence in the Jundee goldfield area. Geological Province: Yilgarn Craton. Serpentite +/- tremolite +/- talc +/- carbonate rocks showing relic cumulate and spinifex textures.. Overlain by Fisher basalt.||||||
39271|Plover formation|24235|5|Briefly described|p298, p299|Jurassic|Jurassic|Informal name - see Plover Formation. Geological Province: Bonaparte Basin.||||||
28288|Plumridge beds|36701|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
37217|Plumridge formation|23989|5|Briefly described|p54 Fig. 46|Cenozoic|Cenozoic|Informal name. Geological Province: Yilgarn Craton||||||03-MAR-10
70444|Plutonic group|61269|6|Mentioned|p85|||Informal name referring to gold deposits.||||||
83648|Point Irwin dyke|73480|5|Briefly described|p216-218|Cambrian|Neoproterozoic|Likely associated with Kuunga Orogeny. Host lithology of biotite migmatite. See also Point Irwin basaltic dyke.|580+/-130 Ma, 1454+/-8 Ma U-Pb zircon maximum age||||Microporphyritic basalt dyke, unmetamorphosed.|
40313|Point Maude Member|24390|5|Briefly described|p20|Late Devonian|Late Devonian|Of the Gneudna Formation.  Geological Province: Southern Carnarvon Basin.||||||
77446|Point Spring Formation|67354|6|Mentioned|p73. |||||Onshore unit in Wadeye Sub-Group.||||
39307|Point Springs Formation|24378|5|Briefly described|p14, p15||Early Carboniferous|Geological Province: Bonaparte Basin.||||||
73559|Point Torment formation|36483|5|Briefly described|p71|||Informal or misspelt - see Point Torment Sand. Geological Province: Canning Basin.||||||
83356|Point spring Sandstone|73117|6|Mentioned|p15|Bashkirian|Serpukhovian|[Probably a variation on Point Spring Sandstone]. Bonaparte Basin, southern. Palynozonation: S. ybertii.||||||
25405|Poison Hill Greensand Member|41989|5|Briefly described|p115|||||||||
74959|Polar Bar Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Pliocene|Pliocene|In Cowan palaeovalley, overlying Yilgarn Craton.||||||08-FEB-10
23913|Pole Group|22534|5|Briefly described|p4, Fig.4 p7|||||||||
23913|Pole Group|22596|6|Mentioned|Fig.9 p419|||||||||
23913|Pole Group|23132|6|Mentioned|p336|||||||||
23913|Pole Group|24139|5|Briefly described|p239 Table 1|||Geological Province: Yilgarn Craton.||||||
23913|Pole Group|42221|5|Briefly described|Table 1 P6|||||||||
23913|Pole Group|42382|6|Mentioned|Table 1 P9|||||||||
23913|Pole Group|42696|6|Mentioned|Plate 1B|||||||||
23913|Pole Group|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
23913|Pole Group|42989|5|Briefly described|Fig.2|||||||||
23913|Pole Group|43074|6|Mentioned|Table 1|||||||||
23913|Pole Group|43101|5|Briefly described|Table 1.|||||||||
23913|Pole Group|43162|6|Mentioned|5|||||||||
23913|Pole Group|43496|6|Mentioned|6|||||||||
23913|Pole Group|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Includes; Missouri Basalt, Wongi Basalt. Overlain by Linger and Die Group. Geological Province: Ora Banda Domain. Consists of tholeiitic and high-Mg basalt flows, subaqueous.||||||11-JUN-15
23913|Pole Group|60627|5|Briefly described|p65 Tb.1|||||||||
23913|Pole Group|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Tholeiitic and komatiitic basalt flows.||||||11-JUN-15
23913|Pole Group|65834|6|Mentioned|p7|||Ora Banda Domain, Kalgoorlie Terrane.|||Missouri, Wongi Basalts.||Tholeiitic and high-Mg basalt flows; subaqueous.|
23913|Pole Group|73391|6|Mentioned|Appendices.|||Witt (1990). Regional stratigraphic correlation chart of other workers.|||Missouri Basalt, Wongi Basalt.|||
78386|Poleile Group|69014|6|Mentioned|Map Legend|||Mis-spelling of Polelle Group.||||||01-MAY-14
34413|Pollick Hills Formation|22716|6|Mentioned|p232|Statherian|Statherian|||||||
74118|Polloch Hills Formation|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Probably misspelt - see Pollock Hills Formation. Of the Mount Webb Suite. Age: 1615Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
81350|Ponton Creek gneiss|70090|5|Briefly described|p444|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton. Of Barren Basin. Mafic magmatism associated with Biranup Orogeny. Depositional environment: moderate energy. Shallow marine? Proximal volcanics? Sedimentary protoliths deposited between 1710 Ma and 1650 Ma during Biranup Orogeny. Metamorphosed to amphibolite to granulite facies. Maximum depositional age: c. 1689+\-6 Ma. Minimum depositional age: contrained by c. 1666+\-12 Ma intrusive monzogranite. Unimodal zircon age component of c. 1690 Ma (volcanic protolith?) indicates EHfi array of -6 to 0, corresponding to 2.4-2.6 Ga model ages. Late Paleoproterozoic detrital age components suggest derivation from local Biranup Zone sources. Shown as Ponton Creek psammitic gneiss p445, 446, 447, 448, 449, 451, 453, 457.|||||Sand and grit-dominated psammitic gneiss.|08-AUG-19
39294|Pool sandstones|24246|6|Mentioned|p14|Permian|Permian|Misspelt - see Poole Sandstone.||||||24-FEB-05
80357|Poole Range Beds|70774|5|Briefly described|p7|||Said to be of Blatchford (1927)[ who actually used Poole Range beds in App. 2 p49]. Obsolete name, after numerous revisions this name was replaced by the Poole Sandstone by Guppy et al., 1951.||||||05-FEB-18
83332|Poole Range Group''|73117|6|Mentioned|p28|||Wade (1936, 1937). [Superseded.  See Poole Sandstone].||||||31-AUG-22
39295|Poole sands|24246|6|Mentioned|p15|||Informal -see Poole Sandstone. Geological Province: Canning Basin||||||24-FEB-05
39284|Poole sandstone|24246|6|Mentioned|p14|||Geological Province: Canning Basin.||||||
39284|Poole sandstone|61139|5|Briefly described|p42 Fig. 4|Early Permian|Early Permian|Geological Province: Canning Basin.||||||
39284|Poole sandstone|69693|5|Briefly described|p3|Sakmarian|Sakmarian|||||Unconformably overlies Carolyn Formation (Grant Group). Is overlain by Noonkanbah Formation.||
33366|Poondano Formation""|24025|5|Briefly described|p17|||Informal name.  Geological Province: Pilbara Craton.||||||
69912|Pooranoo metamorphics|61262|6|Mentioned|p448 Fig. 5c & 5d|||Informal - see Pooranoo Metamorphics.||||||31-JAN-06
34348|Porongurup Pluton|22737|5|Briefly described|9,10|||||||||
41364|Porongurups Granite|50434|5|Briefly described|p3.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Albany-Fraser Province. Of the Nornalup Supersuite. Age: 1184 +/- 11Ma (Shrimp).||||||
81608|Portee Supersuite|72251|6|Mentioned|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton.||||||
38546|Portrea granitoids|23813|6|Mentioned|p90 Tb. 1|Archean|Archean|Misspelt - should be Portree granitoids; not intended as a formal name.  Geological Province: Pilbara Craton.||||||07-NOV-08
38546|Portrea granitoids|23936|5|Briefly described|Tb.1|Archean|Archean|Age: >3.0-2.94 Ga. Geological Province: Pilbara Craton.||||||05-DEC-16
35910|Portree Granite Complex|23348|5|Briefly described|222|Archean|Archean|||||||07-NOV-08
73587|Portree Granitic Complex|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Superseded by Portree Granite (Portree Suite, Sisters Supersuite).||||||07-FEB-11
36849|Portree Granitoid Complex|22906|5|Briefly described|p45, p46 Fig. 1|Archean|Archean|Intruded the Mallina Basin in c.2950Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36849|Portree Granitoid Complex|23743|4|Described|p10|Archean|Archean|Age: c.2945 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
36849|Portree Granitoid Complex|23784|5|Briefly described|p32|Archean|Archean|Age: c.2950Ma.||||||07-NOV-08
36849|Portree Granitoid Complex|23789|5|Briefly described|p6 Tb. 1|Archean|Archean|See also p29.  Geological Province: Pilbara Craton.||||||07-NOV-08
36849|Portree Granitoid Complex|23793|4|Described|p34|Archean|Archean|Age: c.2950Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
36849|Portree Granitoid Complex|23794|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36849|Portree Granitoid Complex|23936|5|Briefly described|Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 2950 Ma.||||||07-NOV-08
36849|Portree Granitoid Complex|24184|5|Briefly described|p716|Archean|Archean|Geological Province: Mallina Basin. Age: 2946 +/- 6Ma (Nelson 1999)||||||07-NOV-08
36849|Portree Granitoid Complex|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Age: ca. 2950 Ma. Geological Province: Mallina basin||||||07-NOV-08
36849|Portree Granitoid Complex|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 2950 Ma||||||07-NOV-08
36849|Portree Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||West Pilbara. Poorly exposed.|||||Foliated monzogranite, granodiorite, migmatite; some porphyritic phases.|
36849|Portree Granitoid Complex|60362|5|Briefly described|p1517, p1518 Fig.2, p1527|Archean|Archean|Mallina Basin. Geochemistry discussed: one sample has an eNd value of +1.1.|||||Felsic alkali granites.|
36849|Portree Granitoid Complex|67201|6|Mentioned|p62 Fig.52, p63 Fig.54|||Mallina Basin. ||||||
36849|Portree Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin|||||Alkali granite; metamorphosed.|03-SEP-14
39768|Portree granitoid|24193|14|Not recorded|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
77570|Potoroo Sandstone|66937|5|Briefly described|p166, pp176-178.|Archean|Archean|c.1160 m thick. Unexposed; known from two drill-cores. Shows upward-thinning and upward-fining of sediment, representing unconfined turbidites in a middle to lower deep-marine fan, in marked contrast with underlying Wallaby Conglomerate.||Unit in Wallaby Supersequence.||Overlies Wallaby Conglomerate.|Graded beds of massive, rarely plane-laminated, fine- and very fine-grained sandstone and plane-laminated siltstone, black shale; rare bedded chert.|
41370|Pottoyu Granitic Complex|24197|5|Briefly described|p97|||Part of the Kulgera Supersuite. Geological Province: Musgrave Block.||||||07-FEB-11
41370|Pottoyu Granitic Complex|50607|5|Briefly described|p1.1, 2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Of the Kulgera Supersuite.  Age: 1192-1144 +/- 13Ma (U-Pb, Rb-Sr).||||||
78634|Powder Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes unnamed leucogabbro unit.||Gabbro; leucogabbro; both metamorphosed.|07-AUG-15
78634|Powder Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro and leucogabbro; metamorphosed.|
78634|Powder Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro and leucogabbro; metamorphosed.|
80942|Powder Sill Gabbro|72049|5|Briefly described|p253, p259, p267|||Affinities with the Williamstown Dolerite.||||Intrudes the Kapai Slate, Kambalda Sequence.|Dolerite.|18-MAR-19
80942|Powder Sill Gabbro|73391|6|Mentioned|p254, 256-257, 259|||Coolgardie Domain. See also references to Powder Sill (p102, 251, 254, 256, 259, 275-276, 304, 362, 366, 374-375, 383, 387, Appendices).||||||
73788|Powder Sill dolerite|60514|6|Mentioned|p62|Archean|Archean|Informal name. Geological Province: Yilgarn Craton.||||||07-FEB-11
25413|Praire Downs Beds|30881|4|Described|p526|||||||||
27542|Prairie Downs Beds|29916|6|Mentioned|p119|||||||||
27542|Prairie Downs Beds|34135|5|Briefly described|Table 2|||Middle Proterozoic. Bangemall Group.||||||
27542|Prairie Downs Beds|36884|5|Briefly described|p151|||||||||
27542|Prairie Downs Beds|36891|4|Described|p443|||||||||
27542|Prairie Downs Beds|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27542|Prairie Downs Beds|38299|6|Mentioned|p12|||||||||
26853|Prairie Downs Formation|42013|5|Briefly described|Map legend|Proterozoic||||||||
26853|Prairie Downs Formation|44142|6|Mentioned|p314 Tb.4-4, p317|||Tyler et al., (1989); formerly Prairie Downs Member. Sandy influxes from alluvial fans.||||||
80101|Preston Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Orosirian|Orosirian|West Pilbara Craton.|1816 Ma|||||
31700|Pricas Creek Group|43818|6|Mentioned|Fig.2.p39||Early Ordovician|Misspelling of Prices Creek Group?||||||
79599|Prince Regent Dyke Suite|70761|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|North Australian Craton.||||||10-NOV-16
79599|Prince Regent Dyke Suite|70826|6|Mentioned|p14 tbl 5|Proterozoic|Proterozoic|Kimberley. Age ranges from 2500-541 Ma [not very useful].||||||20-MAY-20
79599|Prince Regent Dyke Suite|71267|4|Described|GEOL_LUT_CSV files|Carboniferous|Devonian|Events: Western Australian events (4000-0.01 Ma); North Australian Craton events (2500-250 Ma); Alice Springs Orogeny (450-295 Ma). See 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|419.2-298.9 Ma (inferred)||||Dolerite; typically northwesterly trending dykes|
80370|Princess Range Sandstone|67855|5|Briefly described|p209|||Misspelling of Princess Ranges Quartzite. See p208.||Earaheedy Group|||Quartz sandstone with shallow-water structures.|
76846|Princess Ranges Formation|7161|6|Mentioned|p99 Fig.9|||Earaheedy Basin. Less than 800m thick (from p99 Fig.9).||||||
26111|Princess Ranges Quartzite|23529|5|Briefly described|p10|||Downgraded to Member status - see Princess Ranges Member of the Chiall Formation.   Geological Province: Earaheedy Basin||||||
26111|Princess Ranges Quartzite|23589|5|Briefly described|p3|||Now known as Princess Range Member. Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||
26111|Princess Ranges Quartzite|24017|6|Mentioned|p16|||Reduced to member status - see Princess Ranges Member of Chiall Formation.||||||
26111|Princess Ranges Quartzite|30010|6|Mentioned|p45|||||||||
26111|Princess Ranges Quartzite|31217|2|Defined|p42|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
26111|Princess Ranges Quartzite|36551|6|Mentioned|Table 29|||||||||
26111|Princess Ranges Quartzite|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26111|Princess Ranges Quartzite|37300|6|Mentioned|p81|||||||||
26111|Princess Ranges Quartzite|37460|3|Fully described|p142|||||||||
26111|Princess Ranges Quartzite|38515|4|Described|p13|||||||||
26111|Princess Ranges Quartzite|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26111|Princess Ranges Quartzite|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26111|Princess Ranges Quartzite|40355|5|Briefly described|p7|||||||||
26111|Princess Ranges Quartzite|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26111|Princess Ranges Quartzite|40938|2|Defined|p46|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26111|Princess Ranges Quartzite|43595|5|Briefly described|Table 3-9,p346|||||||||
26111|Princess Ranges Quartzite|43652|6|Mentioned|Fig.3,p381|||||||||
26111|Princess Ranges Quartzite|50188|5|Briefly described|p4 Fig. 2|||Written as "Princess Ranges Quartzite". Superseded by Princess Ranges Member when amalgamated along with Wandiwarra Formation into the Chiall Formation after it was recognised that these two units formed a single depositional package mappable as one unit.||||||16-JUL-08
26111|Princess Ranges Quartzite|50222|6|Mentioned|p329|||Superseded by Princess Ranges Member and included in the Chiall Formation (Miningarra Subgroup, Earaheedy Group).||||||
26111|Princess Ranges Quartzite|64285|5|Briefly described|p66 Fig. 1|||Of Bunting (1986). Rocks incorporated into the Chiall Formation and name no longer used.||||||07-FEB-11
26111|Princess Ranges Quartzite|66427|5|Briefly described|p46 Fig.4, p63 |||Former name for the Princess Ranges Member; see references to that unit at p44 Tb.2, p46-48, p63, p66-70.||||||
26111|Princess Ranges Quartzite|67855|5|Briefly described|p208 fig 3-8|Paleoproterozoic|Paleoproterozoic|Misspelt as Princess Range Sandstone p209.||Minningarra Subgroup|||Quartz sandstone with shallow-water structures.|
38135|Princess Ranges Quartzite""|23529|6|Mentioned|p16|||Informal - see Princess Ranges Quartzite, now superseded by Princess Ranges Member.||||||
38135|Princess Ranges Quartzite""|50188|5|Briefly described|p3, p6-7|Paleoproterozoic|Paleoproterozoic|Superseded by Princess Ranges Member.  Now forms part of the Chiall Formation, after downgrading to member status. Geological Province: Earaheedy Basin.||||||07-NOV-08
38135|Princess Ranges Quartzite""|64284|5|Briefly described|p59, p60 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Bunting (1986). Replaced by combination of Princess Ranges Member and part of Wandiwarra Member of the Chiall Formation. Geological Province: Earaheedy Basin||||||07-FEB-11
38135|Princess Ranges Quartzite""|64772|6|Mentioned|p12, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Superseded by Princess Ranges Member of the Chiall Formation.||||||07-FEB-11
41218|Princess Ranges member|50223|6|Mentioned|p346, p355|||Informal - see Princess Ranges Member.||||||
41218|Princess Ranges member|50224|6|Mentioned|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Informal name.  Of the Chiall Formation (Minningarra Subgroup).||||||07-FEB-11
38720|Princess Royal Formation|24397|5|Briefly described|p241|||Not related to North Royal Formation.  Possibly same unit as Princess Royal Spongolite.||||||
38720|Princess Royal Formation|65260|6|Mentioned|p27|Late Eocene|Late Eocene|Spongolitic; interfingers with the Hampton Sandstone.||||||
72755|Princess Royal Spongilite|61814|5|Briefly described|p22|Late Eocene|Late Eocene|||||||08-FEB-10
28943|Prudhoe Deltaics|42053|5|Briefly described|Fig.3 P30|||||||||01-MAR-10
77482|Prudhoe Member|60385|5|Briefly described|p270|Maastrichtian|Campanian|Browse Basin. Shown as at least 3 distinct units in various parts of the Turnstone Formation.||Turnstone Formation|||Sandstone.|01-SEP-14
77483|Puffin Member|60385|5|Briefly described|p269, 270, 271|Campanian|Campanian|Browse Basin. See also Puffin Sandstone, Puffin Sandstone Member.||Of Turnstone Formation?|||Turbidite sandstone.|01-SEP-14
77484|Puffin Sandstone|60385|6|Mentioned|p270, p281|Campanian|Campanian|Name used to describe shallow marine sandstones in the Money Shoal/Arafura basins and Darwin Shelf/Malita Graben but also used for massive submarine fan complexes in Vulcan Sub-basin. See also Puffin Member, Puffin Sandstone Member. ||||||
77484|Puffin Sandstone|64689|6|Mentioned|p14|||May form a stratigraphic trap for Jurassic oil migrating up fault conduits.||||||
77484|Puffin Sandstone|64693|5|Briefly described|p373, p375-376, p388-390 |Maastrichtian|Campanian|Browse Basin, Vulcan Sub-basin. Consists of six main depositional lobes, fed by a series of channels at the foot of a long-acting canyon. Appears as Puffin Formation on p377.||||Overlies Fenelon Formation.|Interbedded deep marine sandstone, fine to coarse, moderately well sorted, often well rounded quartz grains; minor claystone and siltstone.|
77484|Puffin Sandstone|64697|6|Mentioned|p85, p86, p90  |Late Cretaceous|Late Cretaceous|A small gas column was encountered by Citco's Swan-2 in 1980.||||||
77485|Puffin Sandstone Member|60385|5|Briefly described|p272 Fig 3|Campanian|Campanian|Browse Basin. Informal new name. On Figure shown as two parts, both underlying and overlying the Borde Marl Member. See also Puffin Sandstone, Puffin Member.||Turnstone Formation|||Sandstone.|01-SEP-14
72655|Puffin/Prudhoe Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Informal compound term to include both Puffin Formation and Prudhoe Formation.  Age: ~71-~63Ma. Geological Province: Vulcan Sub-basin.||||||
70711|Punkerri Beds''|62453|6|Mentioned|p50|||Informal Name.||||||
23925|Punta Punta Formation|36551|6|Mentioned|Table 22|||||||||
23925|Punta Punta Formation|43862|5|Briefly described|Fig.2 p378|||||||||
23925|Punta Punta Formation|43868|5|Briefly described|Fig.3 p154|||||||||
81609|Pyramide Hill Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Soanesville Group.||Uppermost unit of Soanesville Group. Overlain unconformably by Farrel Quarzite. Underlain by Honeyeater Basalt.||
81609|Pyramide Hill Formation|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane. [Mis-spelling of Pyramid Hill Formation].||Soanesville Group.||Overlies Honeyeater Basalt. Is overlain unconformably by Farrel Quartzite.||
75594|Pyrenees Member (WA)|61555|4|Described|p240||Berriasian|Exmouth Sub-basin. Age based on palynology, dinoflagellates: in P. iehiense 4cib-4cia subzones of Helby. Depositional evironment inner shelf to fluvial. This unit not found in Pyrenees-1.||Of Barrow Group.|||Pebble conglomerate to fine sandstone.|20-MAR-12
75595|Pyrenees Sandstone (WA)|61555|6|Mentioned|p234|||BHP Billiton nomenclature. Replaced by [invalid] Pyrenees Member. ||||||
27225|Quagering Beds|37341|2|Defined|p246|Eocene|Eocene|||||||
27225|Quagering Beds|37350|6|Mentioned|Fig.1|||||||||
80026|Quail Limestone|69297|5|Briefly described|p249|Serpukhovian|Visean|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Overlies the Moogooree Limestone. Unconformably overlain by the Harris Sandstone, Lyons Group.|Siltstones and limestones.|
80090|Quartpot pelite|69596|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Yilgarn Craton.||||||
42403|Quindalup Dune System|23816|5|Briefly described|p255|Recent|Recent|Geological Province: Perth Basin.||||||
42403|Quindalup Dune System|40400|6|Mentioned|p109|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
42403|Quindalup Dune System|61811|5|Briefly described|pp50-52.|Holocene|Holocene|[Formal name is Quindalup Dunes]. Of Grey et al. (1990). Hosts Lake Thetis with growing stromatolites and microbial mats. An egg from the Madagascan Elephant Bird was found in this unit in 1992.||||||
42403|Quindalup Dune System|63745|6|Mentioned|p67|||See also p60 Fig. 1.||||||07-FEB-11
42403|Quindalup Dune System|64635|5|Briefly described|p30-31|Holocene|Holocene|Grey et al.(1990). Hosts the Lake Thetis stromatolites tourist atraction near Cervantes. Also hosted a 2000-year-old egg of the flightless, extinct Madagascan Elephant Bird (Aepyornis maximus).|5600 +/- 260 years BP (Mory, 1995).|||||
42403|Quindalup Dune System|69840|6|Mentioned|p183, p186 Fig.3|Holocene|Holocene|Equivalent to Safety Bay Sand. Parallel to the coast this unit is the most westerly and youngest of three associated dune systems.|||||Carbonate sand.|
42403|Quindalup Dune System|71780|14|Not recorded|p51 Table 1, Plate 2||Quaternary|No white card.||||||
32963|Quindalup System""|44303|14|Not recorded|p.12|||(ref. to McArthur & Bettanay 1960). (I/50-5,9).||||||
25427|Quinnanie Formation|42392|6|Mentioned|Fig.1 P114|||Variation of Quinnanie Shale?||||||
23930|Quinns Basalt|42533|3|Fully described|p69|||Name reserved but Quinns Shale already in database.||||||
23930|Quinns Basalt|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p40|Archean|Archean|Of Murchison Province||Mount Farmer Group||Overlies Windaning Formation.|Silicified, massive, needle-spinifex textured and fine-grained basalt interlayered with basaltic andesite.|
23930|Quinns Basalt|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Interlayered high-Mg and tholeiitic basalt.|
23930|Quinns Basalt|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
23930|Quinns Basalt|72494|6|Mentioned|p22-23|||Superseded: see references to Quinns Basalt Member (p15-18, 21-23, 28).||||||
28259|Quinns Shale Member|23816|6|Mentioned|p242, 246|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Of the Yarragadee Formation. Max. thickness: 57 m.||||||
28259|Quinns Shale Member|24058|6|Mentioned|p122|||Geological Basin: Perth Basin.||||||
28259|Quinns Shale Member|29603|6|Mentioned|p109|||||||||
28259|Quinns Shale Member|29693|6|Mentioned|Fig.7|||||||||
28259|Quinns Shale Member|30188|2|Defined|p74|Neocomian|Neocomian|Refers Bozanic(1969)||||||
28259|Quinns Shale Member|35152|6|Mentioned|p3|||||||||
28259|Quinns Shale Member|35282|6|Mentioned|Fig.10|||||||||
28259|Quinns Shale Member|36293|5|Briefly described|p158|||||||||
28259|Quinns Shale Member|36890|3|Fully described|p246|||||||||
28259|Quinns Shale Member|40300|6|Mentioned|Fig.2|||||||||
28259|Quinns Shale Member|41728|6|Mentioned|p444|||||||||
35639|Rabbit Ears Sandstone|23279|6|Mentioned|p21|||(Bergmark and Evans, 1987).||||||
26862|Radio Hill Complex|23784|5|Briefly described|p12|Archean|Archean|||||||07-NOV-08
26862|Radio Hill Complex|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
26862|Radio Hill Complex|43597|6|Mentioned|p716|||||||||
34313|Radio Hill intrusion|22676|6|Mentioned|p284|||Pilbara Block||||||
81610|Radley Supersuite|72251|6|Mentioned|p54|||Geological province: West Pilbara Superterrane, Pilbara Craton. Poor diagram.||||||03-SEP-19
31104|Raeside Granitoid Complex|43478|2|Defined|p33-62|||||||||
31104|Raeside Granitoid Complex|65147|6|Mentioned|p9 Fig.5|||||||||02-FEB-17
41129|Raeside granite complex|24196|5|Briefly described|p18|Archean|Archean|Age: high-Ca granites 2.76 Ga (Black et al., 2002)||||||07-NOV-08
82963|Raeside granitic complex|73238|5|Briefly described|p6, 9, 12, 27|||Leonora district, Eastern Goldfields Terrane. Is surrounded by Sons of Gwalia shear zone.|c.2760-2740 Ma.||||Granite, granodiorite.|
41128|Raeside granitoid complex|24196|6|Mentioned|p40|||||||||
24468|Ragged Hills Granophyre|23746|6|Mentioned|p7|||||||||
24468|Ragged Hills Granophyre|39697|3|Fully described|p51|||||||||
24468|Ragged Hills Granophyre|41561|6|Mentioned|p545|||Dated at about 2400 Ma.||||||01-AUG-11
24468|Ragged Hills Granophyre|44152|6|Mentioned|p177|||Of Hickman (1983), for two strips of granophyre E of the Gregory Range. Same as Gregory Granitic Complex?||||||23-OCT-15
42474|Rainy Rocks monzogranite|60708|6|Mentioned|p146 Fig. 7|||Informally named for the geographic locality of Rainy Rocks.||||||13-JAN-05
76060|Range Bore intrusion|66195|6|Mentioned|p605|||Former informal name for lower part of Gnanagooragoo Igneous Complex||||||
41238|Ravelstone formation|50226|6|Mentioned|p420|||Informal - see Ravelstone Formation.||||||
41238|Ravelstone formation|61848|6|Mentioned|p300, p301|||Informal - see Ravelstone Formation.||||||
28952|Ravensthorpe Series|31393|6|Mentioned|Pl.25|||||||||
73783|Ravensthorpe quartz diorite|50542|6|Mentioned|p122|||Informal name. Geological Province: Yilgarn Craton.||||||07-FEB-11
30534|Recherche Granite|22448|6|Mentioned|p876|||||||||
30534|Recherche Granite|24165|5|Briefly described|Plate 1|Mesoproterozoic|Mesoproterozoic|||Nornalup Complex.|||Moderately to strongly deformed and recrystallised granite; heterogeneous, even-grained or porphyritic.|
30534|Recherche Granite|24526|5|Briefly described|p105 Fig. 6, p108|Mesoproterozoic|Mesoproterozoic|Of the Nornalup Complex.  Unconformably overlain by Mount Ragged Metasedimentary rocks.  Dykes of this granite cut through the Malcolm Gneiss.  Age: 1330-1288Ma.||||||02-MAR-05
30534|Recherche Granite|43203|5|Briefly described|Map Legend||Proterozoic|Of Nornalup Complex.||||||15-DEC-08
30534|Recherche Granite|43212|6|Mentioned|p7|||Age c.1300 Ma (U-Pb SHRIMP).||||||
30534|Recherche Granite|43498|4|Described|5,7|||ages: 1300 Ma||||||
30534|Recherche Granite|62381|5|Briefly described|p3 Fig.3, p7-8|||Geochemistry suggests either substantial mantle component or short crustal residence time.|1330-1288 Ma.|Unit in Nornalup Complex.||Overlies a gneissic basement, probably equivalent to Malcolm Gneiss. Dykes cut the Malcolm Gneiss.||02-JUL-14
30534|Recherche Granite|63866|4|Described|p190-p191, p193|Ectasian|Ectasian|Nornalup Complex. Subdivided into even-grained and porphyritic units. A granodiorite is dated at 1314 +/- 21 Ma and a porphyritic granite dated at 1330 +/- 14 Ma. |c. 1330-1283 Ma (Nelson, 1996)|||Intrudes the Malcolm Gneiss.|Granitic gneiss, porphyritic granite, granodiorite and equigranular granite.|
30534|Recherche Granite|64580|4|Described|map legend||Mesoproterozoic|Moderately to strongly deformed and recrystallized granite; heterogeneous; even grained or porphyritic.||||||15-DEC-08
30534|Recherche Granite|64722|5|Briefly described|Fig. 2 p3-6, p18-19, 28|Ectasian|Ectasian|Intruded into Albany-Fraser Orogen at 1330-1280 Ma. Unconformably overlain by Mount Ragged metasedimentary rocks.||||Intruded into Nornalup Complex.||11-APR-12
30534|Recherche Granite|65487|6|Mentioned|p1, p9|Mesoproterozoic|Mesoproterozoic|Myers (1995), Nelson et al. (1995), Clark (1999). Renamed as the Recherche Supersuite.||||||
30534|Recherche Granite|67581|6|Mentioned|p44 Fig.8||||1330-1280 Ma.|||||
30534|Recherche Granite|68100|6|Mentioned|p35|Mesoproterozoic|Mesoproterozoic|See also Recherche Supersuite, same page.|1330-1280 Ma|||||
30534|Recherche Granite|68186|6|Mentioned|p4, p27|||Myers (1995). Subsequently renamed the Recherche Supersuite.||||||
30534|Recherche Granite|69152|5|Briefly described|500k_geologyp08_lut||Mesoproterozoic||||||moderately to strongly deformed and recrystallized granite; heterogeneous; even grained or porphyritic|
30534|Recherche Granite|69252|6|Mentioned|p4 Fig.1, p20|||Myers (1995). Subsequently the Recherche Supersuite.||||||
30534|Recherche Granite|69559|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic||||||Moderately to strongly deformed and recrystallized granite; heterogeneous; even grained or porphyritic.|
30534|Recherche Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, felsic gneiss|
30534|Recherche Granite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. Of Nornalup Complex.|||||Moderately to strongly deformed and recrystallised granite; heterogeneous; even grained or porphyritic|
31153|Recherche Granite Complex|43498|6|Mentioned|6, 7|||U-Pb ages: 1560, 1810, 2035, 2175, 2735 Ma||||||
75352|Red Hill Formation (WA)|24140|5|Briefly described|p217 Fig. 2|Archean|Archean|Misspelt? probably intended as Red Hill Volcanics.||||||25-JUN-09
26867|Red Hill Granitoid Complex|9766|5|Briefly described|Map Legend|Archaean|Archaean|Syenogranite, monzoreanite porphyry and granodiorite porphyry.||||||
26867|Red Hill Granitoid Complex|41771|5|Briefly described|p30|||||||||
26867|Red Hill Granitoid Complex|42221|6|Mentioned|p30|||||||||
26867|Red Hill Granitoid Complex|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
26867|Red Hill Granitoid Complex|42724|5|Briefly described|map legend|Archean||||||||07-NOV-08
26867|Red Hill Granitoid Complex|42817|5|Briefly described|p18|||see also Table 2||||||
26867|Red Hill Granitoid Complex|43052|5|Briefly described|Fig.3.8|||||||||
26867|Red Hill Granitoid Complex|43102|5|Briefly described|Fig.3|||||||||
26867|Red Hill Granitoid Complex|43162|6|Mentioned|16|||||||||
26867|Red Hill Granitoid Complex|43496|6|Mentioned|15|||Age: 2662+/-6Ma||||||
26867|Red Hill Granitoid Complex|60076|5|Briefly described|p13 Fig. 5, p46 App. 1|||[AgRH]   Syenogranite, monzogranite porphyry and granodiorite porphyry.||||||
26867|Red Hill Granitoid Complex|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean|Superseded by Red Hill Granite?|||||Syenogranite, monzogranite, granodiorite; mafic granite.|07-AUG-15
28957|Red Hill Sandstone""|23815|6|Mentioned|p278|||Superseded by Harris Sandstone (Condon, 1954). Geological Province Carnarvon Basin.||||||
28957|Red Hill Sandstone""|36890|6|Mentioned|p278|||Renamed Harris Sandstone||||||
80213|Red Hill porphyry|71166|5|Briefly described|p30|||Informal name. Hosts gold mineralisation in intruding quartz veins. Kanowna gold camp. Eastern Goldfields Superterrane.||||||05-OCT-17
38693|Red Hill volcanics|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of Whim Creek Group.  Formerly grouped with Mons Cupri dacite as Mons Cupri Volcanics.  Max. thickness: 290m.  Geological Province: Pilbara Craton.||||||07-NOV-08
38693|Red Hill volcanics|24140|5|Briefly described|p216, p221|||Informal - see Red Hill Volcanics. Of Whim Creek Group.  Max. thickness: 290m.  See also p217 Fig. 2.||||||14-SEP-05
69726|Red Hill volcanics Formation|24140|6|Mentioned|p216, p221|||Informal - see Red Hill Volcanics.||||||
69727|Red Hill volcanics formation|24140|6|Mentioned|p217|||Informal - see Red Hill Volcanics.  See also Red Hill volcanics Formation.  Age: 3009+/-4 Ma (Nelson 1998).||||||
80464|Red Rock beds|44140|5|Briefly described|p293-297, p299|Paleoproterozoic|Paleoproterozoic|More than 2000 m thick; fluvial, locally derived from the Lamboo Complex. Parent possibly Speewah Group.||||Unconformable between Halls Creek Group and Mount Parker Sandstone. Intruded by Fish Hole Dolerite. Correlated with Speewah Group or in part with Kimberley Group.|Quartz sandstone, red siltstone, conglomerate.|
38662|Redcastle granite|23786|5|Briefly described|p34 Tb. 4|||Informal name.  Geological Province: Yilgarn Craton.||||||
81581|Redeemer Dolerite|72057|4|Described|p238,243-244,247-248|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Best studied on the western side of the Lawlers anticline, Agnew Greenstone Belt. Can be traced in regional geophysics around large-scale folds for >50 km. Drill core thicknesses: 30-125m. U-Pb TIMS age of 2686.8+\-3 Ma from zircons extracted from granophyre (Hayman et al., 2015).||||Underlain or overlain by Scotty Creek Sandstone??|Basalt, dolerite and gabbroic lithofacies.|07-FEB-20
81581|Redeemer Dolerite|73151|5|Briefly described|p5, p10, p12 Tb.3|||Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||||Overlies the Agnew Komatiite, Burrell Well Basalt, underlies the Redeemer Basalt, unconformably underlies the Scotty Creek Formation.|Dolerite.|
83955|Redeemer Formation|70863|6|Mentioned|p16|||Hayman et al. (2015). Yilgarn Craton.|||||Tholeiitic basalts.|
75175|Reedys Trondhjemite|64891|5|Briefly described|p37 Fig. 2|Archean|Archean|Probably misspelt in the figure - see Reedy Trondhjemite.||||||07-FEB-11
82956|Reeves formation|69693|6|Mentioned|p4|||||||||
33911|Regal Basalt|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3000 Ma||||||07-NOV-08
33911|Regal Basalt|66118|6|Mentioned|p147, p153|||Regal Terrane. See also Regal Formation in this paper.|c. 3200 Ma, Nd model age|||||
74800|Revolver Creek Dolerite|64589|6|Mentioned|sample_locations file|||Sample locations.||||||12-NOV-08
35850|Revolver Creek dolerite|23328|5|Briefly described|1031 Fig.3|||||||||07-SEP-09
72623|Rhaetian Marl|24351|5|Briefly described|Plate 4 (in pocket)|Late Triassic|Late Triassic|Geological Province: Exmouth Plateau.||||||13-DEC-07
72623|Rhaetian Marl|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Age: >205Ma. Geological Province: Exmouth Plateau.||||||
41466|Richenda Granite|50437|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1858 +/- 5Ma (Shrimp). Used interchangeably with Richenda Microgranodiorite.||||||07-NOV-08
76818|Richenda Microgranite|64730|6|Mentioned|p141|Orosirian|Orosirian|Undeformed.|1858 +/- 5 Ma (Griffin et al., 1993).|||?Intrudes Marboo Formation.||03-MAY-12
76818|Richenda Microgranite|72437|5|Briefly described|p34-35|||Whole-rock analyses are provided.|||||Micro-granodiorite.|
70571|Ridge Apron Facies|61521|5|Briefly described|p4 Tb.1||Holocene|Not a formal name. Eroded Pleistocene aeolinite derived from the Tamala Limestone.||||||02-JUN-06
77194|Rim Sandstone Member|44139|6|Mentioned|p281, Table 3-15|Proterozoic|Proterozoic|Of Upper Malu Formation. Informal name (of Turner 1983 PhD thesis). Now included in Telfer Formation| | ||||10-SEP-12
25443|Ringa gneiss|38789|6|Mentioned|Table 2|||||||||
40340|Robe Formation|24573|5|Briefly described|p669|Middle Miocene|Late Oligocene|Formerly the Robe Pisolite"". Geological Province: Hamersley Province||||||
40340|Robe Formation|60539|5|Briefly described|p518|||Possibly not Eocene in age.||||||
40340|Robe Formation|63432|5|Briefly described|p736 Fig. 2|||Replaced Robe Pisolite?||||||07-FEB-11
40340|Robe Formation|65194|5|Briefly described|p101, p102, p104, p106, p113-114|Late Eocene|Late Eocene|Formerly Robe Pisolite: see also p15 Fig.2.3, p16 Fig.2.4, p.99.Fluvial. Unconformably overlain by the Millstream Dolomite, Kangiani Clay. Massive ironstone, cemented pisoliths, and layers of clay and shale with pebbly shale common at the base. Fortescue Palaeovalley aquifer.||||Overlies Marra Mamba Iron Formation, Wittenoom Dolomite, Yarraloola Conglomerate.||11-APR-16
40340|Robe Formation|69538|5|Briefly described|p522 Fig.5, p557, p583-585|||Formerly the Robe Pisolite in the Robe area. Billions of tonnes of channel iron deposits.|||||Pedogenic pelletoids and peloids; clay.|
40340|Robe Formation|71808|6|Mentioned|p117|||||||||
40340|Robe Formation|72447|6|Mentioned|p237-238|||Hamersley Region. Hosts fossiliferous iron-rich pisolitic deposits (channel iron deposits). Sourced from Hamersley Group BIFs.||||||
40340|Robe Formation|73574|5|Briefly described|p762|Miocene|Late Eocene|Western Hamersley region. See also Robe Pisolite.||||Overlies Munjina Member|Thick unit dominated by pisoids and pelletoids.|
78788|Robe Pisolite Formation|63153|6|Mentioned|p1359, p1370 |||One of the colluvial and alluvial detrital components of the buried valley to the N of the Hope Downs ore deposit. They collectively constitute a probable future resource.||||||
78788|Robe Pisolite Formation|72447|6|Mentioned|p238-239|||Hamersley Province.||||Equivalent to Poondano Formation.||
40339|Robe Pisolite""|24573|5|Briefly described|p669|Middle Miocene|Late Oligocene|Superseded by the Robe Formation. Geological Province: Pilbara Craton||||||
40339|Robe Pisolite""|63432|6|Mentioned|p734|||Name given to iron-rich fluvial rocks (channel iron deposits) ranging from gravelly mudstones to fine gravel, and subordinate pebble to boulder conglomerates - also known as "pisolite ore" or "limonites".||||||07-FEB-11
74198|Robe River alluvium|36268|6|Mentioned|p176|||Aquifer at Pannawonica.||||||
23941|Robert Beds|45149|2|Defined|p23|Mesoproterozoic|Mesoproterozoic|See also Table 1.||||||
23941|Robert Beds|46975|6|Mentioned|p83|||||||||
23941|Robert Beds|62453|6|Mentioned|p15|||Upgraded to Robert Formation.||||||
70712|Robert Beds''|62453|6|Mentioned|p15|||Now Robert Formation.||||||
70714|Robert Formation''|62453|6|Mentioned|p15|||Now Robert Formation.||||||
70713|Robert beds''|62453|6|Mentioned|p27|||Informal name. Probably superseded by Hussar Formation.||||||
25447|Robinson Range Beds|29663|6|Mentioned|p52|||||||||
25447|Robinson Range Beds|30951|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25447|Robinson Range Beds|31815|3|Fully described|p96|||?equiv. Mt. Bruce Supergroup. See also Plates 26-29, P101.||||||
25447|Robinson Range Beds|31940|4|Described|p10|||Archaean||||||
25447|Robinson Range Beds|35269|6|Mentioned|p307|||||||||
25447|Robinson Range Beds|36870|5|Briefly described|p60|||||||||
25447|Robinson Range Beds|41066|6|Mentioned|1 of 2 I02|||||||||
25447|Robinson Range Beds|45086|6|Mentioned|p21|||Lithology.||||||
25447|Robinson Range Beds|49896|5|Briefly described|p2 Tb. 1|||Of MacLeod (1970). Superseded by Robinson Range Formation.||||||
83389|Robinson's Komatiite|73391|5|Briefly described|p132-133, 282|||Kanowna district; north of the Fitzroy Fault. 1000m thick.||||Is faulted under, and locally unconformably overlain by, Ballarat member.|Ultramafic rocks.|
38989|Rocky's Reward ultramafic unit|23862|5|Briefly described|p31 Tb. 1|||Not intended as a formal name.  Possibly part of Perseverance Ultramafic Complex?||||||
38989|Rocky's Reward ultramafic unit|69414|6|Mentioned|p86|Archean|Archean|Agnew-Wiluna Greenstone belt, Yilgarn Craton. Agnew Domain, Yilgarn Craton.|2720 +/- 14 Ma (Nelson, 1997).|||||
38989|Rocky's Reward ultramafic unit|70275|5|Briefly described|p477, 481, 485-488, 490-491, 495, 499|||Leinster area, Agnew-Wiluna Belt, Yilgarn Craton. Also appears as Rocky's Reward Ultramafic Unit. North-over-south thrusting produced duplication in the Rocky's Reward pit. Structurally bound slices of ultramafic rock extend c.15 km along strike. Mineralisation described in detail.|||||A lower olivine cumulate unit overlain by thin, spinifex-textured komatiite flow units; intimately associated with black shales, cherts, and exhalative massive Fe sulfide horizons. Hosts massive Ni sulfide mineralisation.|
72546|Rockys Reward mica schist|69414|6|Mentioned|p88|Archean|Archean|Is presented as Rocky's Reward Feldspar-quartz-mica Schist.||||||
34386|Roebourne Belt volcanics|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3270-3200Ma||||||07-NOV-08
34457|Roebuck Dolomite""|22765|6|Mentioned|P7|||||||||
78427|Rollo's Bore Beds|65194|6|Mentioned|p137|Early Oligocene|Late Eocene|Of Playford et al. (1975) for ancient valley fills or deep lead sediments at Coolgardie and elsewhere in the eastern Goldfields. Subsequently Rollo's Bore Formation (Cockbain and Hocking 1989).||||||
78428|Rollo's Bore Formation|65194|6|Mentioned|p137|Early Oligocene|Late Eocene|Of Cockbain and Hocking (1989); formerly Rollo's Bore Beds of Playford et al. (1975) for ancient valley fills or deep lead sediments at Coolgardie and elsewhere in the eastern Goldfields.||||||
28978|Rottnest Sandstone|32750|6|Mentioned|p313|||Strat. table||||||
73506|Round Hummock Dolerite Suite|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: c. 755Ma. Dolerite or gabbro dyke.||||||
73506|Round Hummock Dolerite Suite|63420|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite dyke , fine- to medium-grained.||||||07-NOV-08
73506|Round Hummock Dolerite Suite|63441|5|Briefly described|p13 tb. 2|Archean|Archean|Geological province: Pilbara Craton.||||||07-FEB-11
73506|Round Hummock Dolerite Suite|64621|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: <755Ma. Dolerite dyke , fine to medium-grained.||||||
73506|Round Hummock Dolerite Suite|64654|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Dolerite dyke; fine to medium grained.||||||
73506|Round Hummock Dolerite Suite|64657|5|Briefly described|Map Legend|Neoproterozoic III|Neoproterozoic III|Dolerite dyke; fine to medium grained.||||||
73506|Round Hummock Dolerite Suite|65724|5|Briefly described|map legend|Neoproterozoic|Neoproterozoic|Dolerite dyke (fine to medium grained) and gabbro dyke.||||||
73506|Round Hummock Dolerite Suite|65727|5|Briefly described|Map legend|Proterozoic|Proterozoic|This unit was named Round Hummock dyke swarm in Version 1 of this map sheet.|||||Dolerite dyke, fine- to medium-grained.|
73506|Round Hummock Dolerite Suite|65827|4|Described|Tb.3 p12, p43|Cryogenian|Cryogenian|c. 755 Ma. Intrudes Fortescue Group. Unmetamorphosed, linear (NW to NNW-trending) mafic dykes (dolerite and gabbro) up to 10m wide; associated with copper mineralisation. Appears to be related to the Mundine Well dyke swarm in Yule Granitic Complex.||||||
73506|Round Hummock Dolerite Suite|65829|3|Fully described|p10, p28. |Proterozoic|Proterozoic|Linear dykes up to 15 m wide, trending NW to WNW, postdate the folding and most faulting in the Fortescue Group. Might be a conjugate set with the NNE-trending Mundine Well Dolerite Suite. Quartz veins within the sheared margin of a gabbro dyke host the Meentheena copper prospect.|c.755 Ma.|||Intrudes Fortescue Group and Yilgalong Granitic Complex.|Several medium- to coarse-grained unmetamorphosed dolerite dykes; an unusual totally altered gabbro dyke, coarse-grained, pale grey, good textural preservation.|
73506|Round Hummock Dolerite Suite|66108|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Dolerite dyke, fine- to medium-grained.||||||
73506|Round Hummock Dolerite Suite|66217|5|Briefly described|p5, p6 Table 1, pp55-56.|Cryogenian|Cryogenian|This article says "cf. Round Hummock Suite, Hickman 1983", implying that may be this unit's former stratigraphic name. NW-striking intrusions, unmetamorphosed and postdate folding of the Fortescue Group. Associated with Cu mineralisation to the east of this map area.|c.755 Ma.|||Cross-cuts the Mundine Well dyke swarm (presumably the Mundine Well Dolerite Suite is meant).|Linear, mafic dykes.|
73506|Round Hummock Dolerite Suite|68281|5|Briefly described|Map Legend|Proterozoic|Proterozoic||||||Dolerite dyke; fine to medium grained.|23-SEP-13
73506|Round Hummock Dolerite Suite|68282|5|Briefly described|Map Legend||||||||Dolerite dyke, fine to medium grained.|
73506|Round Hummock Dolerite Suite|68283|5|Briefly described|Map Legend|Proterozoic|Proterozoic||||||Dolerite dyke, fine to medium grained.|
73506|Round Hummock Dolerite Suite|69012|5|Briefly described|Map Legend||||||||Dolerite dyke, fine to medium grained.|29-APR-14
73506|Round Hummock Dolerite Suite|69013|5|Briefly described|Map Legend|Proterozoic|Proterozoic||||||Dolerite dyke, fine to medium grained.|16-NOV-16
73506|Round Hummock Dolerite Suite|69015|5|Briefly described|Map Legend||||||||Dolerite dyke, fine to medium grained.|02-MAY-14
73506|Round Hummock Dolerite Suite|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic||||||Dolerite dyke, fine to medium grained.|
73506|Round Hummock Dolerite Suite|69590|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv.|1000-541 Ma (inferred)||||Dolerite dyke, fine to medium grained|
73506|Round Hummock Dolerite Suite|70826|6|Mentioned|p14 tbl 5|Cambrian|Neoproterozoic|Pilbara Craton. [age range is quite large, may not be useful]|1000-541 Ma|||||
73506|Round Hummock Dolerite Suite|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||dolerite|
36953|Round Hummock Suite|23585|6|Mentioned|p23|||||||||
36953|Round Hummock Suite|23757|6|Mentioned|p15|||Of Hickman (1986).||||||
36953|Round Hummock Suite|24531|6|Mentioned|p11 Tb. 2|||||||||
36953|Round Hummock Suite|50189|5|Briefly described|p27|Proterozoic|Proterozoic|Fine-grained dolerite dykes intruding the granitoid complexes and the Warrawoona Group.||||||
36953|Round Hummock Suite|50544|6|Mentioned|p61|||||||||
36953|Round Hummock Suite|64384|6|Mentioned|p91|||Of Hickman and Lipple (1978).||||||07-FEB-11
36953|Round Hummock Suite|65827|6|Mentioned|p43|Cryogenian|Cryogenian|Former name of Round Hummock Dolerite Suite.
||||||
75814|Round Hummock dyke swarm|64936|5|Briefly described|map legend|Proterozoic|Proterozoic|Dolerite dyke, generally west-northwest trending.||||||
75814|Round Hummock dyke swarm|65726|5|Briefly described|Map legend|Proterozoic|Proterozoic||||||Dolerite and gabbro dykes.|
79144|Rowley Volcanics|13255|6|Mentioned|p369|Middle Triassic|Middle Triassic|Rowley Sub-basin, Roebuck Basin.||||Is interbedded with Locker Shale.||
32579|Royal Amphibolite|45543|4|Described|p.101,105||Archean|Unit of Woolyeenyer Group.||||||07-NOV-08
77538|Royal Sequence|66880|6|Mentioned|pp28-29.|Archean|Archean|See also Royal Sandstone. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank.|2658 +/- 15 Ma.|||||01-NOV-12
77566|Royal Supersequence|66937|5|Briefly described|p155, pp170-172.|Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin. Poorly exposed. Lithofacies stacking is aggradational. Has quartz veining and heterogeneous schistosity.|||||Quartz-sericite or quartz-chlorite schist. Black shale dominant, with sandstones and bedded chert; minor conglomerate in drill core|05-NOV-12
77566|Royal Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
80533|Ruby Limestone|13615|6|Mentioned|p103 App.3|||Said to conformably underlie Abdul Sandstone.||||||09-FEB-19
37089|Rudall Complex""|23742|6|Mentioned|p4|||||||||
37089|Rudall Complex""|49895|6|Mentioned|p5|Proterozoic|Proterozoic|Informal - see Rudall Complex. Geological Province: Paterson Orogen.||||||
29958|Rudall Metamorphic Complex""|43055|6|Mentioned|p26|||Synonym for Rudall Complex.||||||
39741|Rudell Complex|24194|6|Mentioned|p900, p903 Tb.3|||Misspelt - see Rudall Complex. Geological Province: Paterson Orogeny||||||
39734|Ruth Well komatites|24192|6|Mentioned|p862|Archean|Archean|Geological Province: Pilbara Craton. Not intended as a formal name - see Ruth Well Formation. Age: ca. 2.9 Ga (Meisel et al, 2001)||||||07-NOV-08
74142|Ryan's Well Granite|62107|6|Mentioned|p1391 Fig. 2|||Spelling is informal. In the Yandal belt.||||||20-FEB-08
80177|Sabina formation|67925|6|Mentioned|ES p6, Ch8 p5, Ch8 p11-p12|||||||||
28219|Sadler Formation|23294|14|Not recorded|p45||Late Devonian|Has yielded ostracods.||||||
28219|Sadler Formation|24000|5|Briefly described|p348 Fig. 2|Frasnian|Frasnian|Probably misspelt- see Sadler Limestone.  Geological Province: Canning Basin.||||||
28219|Sadler Formation|32141|6|Mentioned|p146|||||||||
28219|Sadler Formation|33042|6|Mentioned|p738|||See also P745||||||
28219|Sadler Formation|34484|6|Mentioned|p21|||||||||
28219|Sadler Formation|38263|6|Mentioned|p16|||||||||
28219|Sadler Formation|39796|6|Mentioned|Map legend|Devonian|Devonian|||||||
28219|Sadler Formation|40236|6|Mentioned|p131|||||||||
28219|Sadler Formation|41215|6|Mentioned|Fig.14|||||||||
28219|Sadler Formation|41492|5|Briefly described|p114|||||||||
28219|Sadler Formation|42994|6|Mentioned|p10|||||||||
28219|Sadler Formation|44403|2|Defined|opp.p.6, Tb.1||Frasnian|E/51-12. Frasnian clastic limestones, bioherms, massive reefs, sandy and silty limestone, siltstone. fossils silicified. Unconformably U/lain Pillara Formation. Conformably O/lain by Mt. Pierre Group.||||||
28219|Sadler Formation|44404|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
28219|Sadler Formation|44993|14|Not recorded|p.26|||||||||
28219|Sadler Formation|44998|2|Defined|p.41||Frasnian|u. Frasnian. Contemp.with part of Pillara Formation. Lowest unit of Mt. Pierre Group. See also p36-7,40.||||||
28219|Sadler Formation|45015|5|Briefly described|p47|Frasnian|Frasnian|Correlated with Gneudna Formation, W.A.  Geological Province: Fitzroy Basin.||||||01-JUN-06
28219|Sadler Formation|45041|6|Mentioned|Fig.45|||Devonian||||||
28219|Sadler Formation|48831|14|Not recorded|p.59,61-67,70,84|||||||||
28219|Sadler Formation|48848|14|Not recorded|p.43,67,78,81|||||||||
28219|Sadler Formation|50150|5|Briefly described|p7, p324|Frasnian|Frasnian|See also p110. Geological Province: Canning Basin.||||||
28219|Sadler Formation|64502|5|Briefly described|p764, p765 Fig. 2|Frasnian|Givetian|||||||
28219|Sadler Formation|66127|6|Mentioned|p49.|||Of Guppy et al. (1958); subsequently renamed Sadler Limestone (Playford and Lowry 1966) to reflect the dominant and characteristic lithology.||||||
68023|Sadler-Pillara Limestone|50150|5|Briefly described|p110|Frasnian|Frasnian|Informal grouping of two units - Sadler Formation and Pillara Limestone. Geological Province: Canning Basin.||||||
25460|Safety Bay Formation|40314|6|Mentioned|Table 2|||||||||
25460|Safety Bay Formation|40367|6|Mentioned|p82|||Probably misspelt - see Safety Bay Sand.||||||07-AUG-07
73791|Safety Bay Sands|60556|5|Briefly described|p22|||||||||
39665|Sahara formation|24449|5|Briefly described|p745|||Informal - see Sahara Formation.  Of the Carribuddy Group.  Geological Province: Canning Basin.||||||
31699|Sahava Formation|43818|6|Mentioned|Fig.2.p39||Silurian|Misspelling of Sahara Formation?||||||
23951|Sahul Formation|41436|6|Mentioned|p44|||||||||
23951|Sahul Formation|41733|6|Mentioned|Fig.3|||||||||
23951|Sahul Formation|42081|5|Briefly described|Fig.2 P291|||||||||
23951|Sahul Formation|42442|6|Mentioned|Fig.3 P4|||Superseded by Sahul Group.||||||
42507|Sahul Shoals|24206|5|Briefly described|p229, P227 Fig. 1|||In the Northwest Shelf area.  Geological Province: Ashmore Platform.||||||05-MAY-05
42507|Sahul Shoals|49637|6|Mentioned|Fig.5|||Informal term. See also Fig. 6.||||||07-FEB-11
73869|Salgash Group|24590|6|Mentioned|p38|||Misspelt - should be Salgash Subgroup.||||||07-FEB-11
40191|Salgash Subgroup, upper|24182|6|Mentioned|p92|||Informal - see Salgash Subgroup.  Geological Province: Pilbara Craton.||||||
40191|Salgash Subgroup, upper|24590|6|Mentioned|p82|||Informal - see Salgash Subgroup.||||||07-FEB-11
68814|Sally Downs Granite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province: Halls Creek Inlier. Name written as Sally Downs only under heading for GRANITE.||||||07-NOV-08
74106|Sally Downs Suite|24197|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Type example of the Sally Downs Supersuite. In the east Kimberley region.||||||07-FEB-11
31882|Sally Downs supersuite|22547|4|Described|p21||Orosirian|Within the Lamboo Complex, Halls Creek Orogen. Age: 1835- 1830 Ma. Previously "Bow River Granitoid Suite", previously "Bow River Granite"||||||14-NOV-06
31882|Sally Downs supersuite|22754|4|Described|p6, p7, p8|Paleoproterozoic|Paleoproterozoic|Age: 1835-1805 Ma.||||||07-NOV-08
31882|Sally Downs supersuite|23323|6|Mentioned|p456 Tb. 1|||Informal - see Sally Downs Supersuite. Includes Mount Christine Granitoid and Sally Downs Tonalite.||||||07-FEB-07
31882|Sally Downs supersuite|23383|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Elsewhere referred to as Sally Downs Supersuite.  Age 1835-1805 Ma.||||||07-NOV-08
31882|Sally Downs supersuite|23599|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Age: c.1835-1805 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
31882|Sally Downs supersuite|23621|6|Mentioned|p53|||||||||
31882|Sally Downs supersuite|23751|4|Described|p16|Paleoproterozoic|Paleoproterozoic|Age: 1830-1800 Ma.||||||07-NOV-08
31882|Sally Downs supersuite|24173|5|Briefly described|p7, p12 Tb.2|Paleoproterozoic|Paleoproterozoic|Informal name. Geol.Prov: Halls Creek Orogen. Of Bow River Batholith. Equivalent to Sally Downs Batholith of Sheppard et al (1995), represented by Loadstone Monzogranite, Shepherds Bore Plutonic Complex and unnamed granite and gabbro. Age: 1832-1810Ma.||||||07-NOV-08
31882|Sally Downs supersuite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal name.  Age: 1835-1805Ma.  In the Bow River batholith.||||||07-NOV-08
31882|Sally Downs supersuite|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31882|Sally Downs supersuite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|Informal||||||
31882|Sally Downs supersuite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
31882|Sally Downs supersuite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Comprises six granitoid units.  Age: 1835-1805Ma. Part of the Bow River batholith.||||||07-NOV-08
31882|Sally Downs supersuite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31882|Sally Downs supersuite|65409|5|Briefly described|pp56-57. |Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen. Part of the Bow River batholith; broadly coeval intrusions of granitic and gabbroic magmas.  Equivalent to 'Sally Downs batholith' of Shepperd et al.  (1995).|1835-1800 Ma.|||||20-FEB-17
31882|Sally Downs supersuite|66845|4|Described|p535, p537 Fig.3, p538, p539, p541, p543|Paleoproterozoic|Paleoproterozoic|Intrudes all 3 zones/terrains (mainly Central zone) of Lamboo Complex from c. 1820 Ma onwards, and marks amalgamation of the terranes. Three suites have overlapping age ranges, contrasting mineralogies and chemical compositions. The Sally Downs supersuite represents a major episode of granite magmatism that is signicantly younger than the Paperbark supersuite.|1835-1805 Ma|Bow River batholith|Kevins Dam suite, Syenite Camp suite and Mabel Downs suite||I-type granites; tonalite and high-K granite|
31882|Sally Downs supersuite|66846|4|Described|p547-559, p548 Fig.1, p549 Fig.2|Orosirian|Orosirian|Granites and gabbros of this suite intrude all three parts of the Lamboo Complex. Granites considered to be primary, crustally derived  melts. Age range probably from U-Pb SHRIMP dating of zircon (see p547). Together with the Paperbark supersuite are part of the Bow River batholith. Rare earth element abundances given on p551 Tb. 2.|1835-1805 Ma|Bow River batholith|Includes the Mabel Downs, Syenite Camp and Kevins Dam suites, plus unnamed gabbros and hybrid rocks.||Tonalite and quartz diorite; monzogranite and syenogranite; granodiorite, tonalite and monzogranite. Intrusions of coeval gabbro and hybrid rock are also included in the supersuite.|
31882|Sally Downs supersuite|72437|4|Described|p9-11, p13, p93, p109|Palaeoproterozoic|Palaeoproterozoic|Intrudes primarily the central zone of the Lamboo Complex. Each of the constituent suites is accompanied by coeval gabbro intrusions. Previously referred to as the Sally Downs batholith by Sheppard et al (1995). Whole rock and REE analyses are provided.|c. 1835-1805 Ma||Includes the Mabel Downs suite, Syenite Camp suite and the Kevins Dam suite.|Intrudes the Amhurst Metamorphics.|Granitoid and coeval gabbro.|
81432|Sally Malay Intrusion|70731|5|Briefly described|p270|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Mafic-ultramafic intrusion emplaced within Tickalara Metamorphics c. 1845 Ma toward the end of the Hooper Orogeny (Page and Hoatson, 2000; Trudu and Hoatson, 2000).|c. 1845 Ma|||||21-AUG-19
81432|Sally Malay Intrusion|71873|6|Mentioned|p426-427|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Nomenclature replaced by the new 'Sally Malay Complex' name introduced in this study.||||||
76770|Sally Malay intrusion|60498|5|Briefly described|p1016 Fig.1, pp1017-1020.|Paleoproterozoic|Paleoproterozoic|Intrusions form dipping sheets, basins. Indicated resource of 3.7 Mt of 1.7 %Ni, 0.7% Cu, and 0.09%Co defined in a possible feeder conduit. Electron microprobe geochemical analyses of apatites and biotites are detailed.|1846 +/- 5 Ma;1844 +/- 3 Ma (Page & Hoatson 2000)||||Layered mafic-ultramafic intrusion: olivine gabbro, troctolite, gabbro, gabbronorite, norite, anorthositic gabbro, anorthosite, lherzolite, dunite.|03-JAN-18
76770|Sally Malay intrusion|63866|5|Briefly described|p131, p138|Orosirian|Orosirian|Central Zone, Halls Creek Orogen.|c. 1845 Ma (U-Pb, Page and Hoatson, 2000)|||||
76770|Sally Malay intrusion|64722|6|Mentioned|p22|Orosirian|Orosirian|Informal name. Mafic-Ultramafic intrusion. Of Halls Creek Orogen.|1840 Ma.|||||11-APR-12
76770|Sally Malay intrusion|69003|6|Mentioned|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Now referred to as Savannah intrusion.||||||
31797|Sally Malay intrusions|43854|5|Briefly described|Map Legend||Proterozoic|||||||
31797|Sally Malay intrusions|43855|5|Briefly described|Map Legend||Proterozoic|||||||
31797|Sally Malay intrusions|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
31797|Sally Malay intrusions|44868|5|Briefly described|Map Legend||Proterozoic|||||||
31797|Sally Malay intrusions|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Layered mafic-ultramafic intrusions; peridotite, troctolite, gabbro, olivine gabbro, olivine gabbronorite, gabbronorite, leucogabbro, and anorthosite; minor chromitite layers.||||||15-DEC-08
31797|Sally Malay intrusions|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Replaced by Sally Malay Suite?|||||Layered mafic-ultramafic intrusions; peridotite, dunite, wehrlite, harzburgite, troctolite, olivine gabbro, olivine gabbronorite, gabbronorite, and olivine leucogabbro.|04-AUG-15
31797|Sally Malay intrusions|71113|6|Mentioned|p96|||Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. See Sally Malay Suite.||||||
31797|Sally Malay intrusions|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Layered mafic-ultramafic intrusions; Olivine gabbro, olivine gabbronorite, gabbronorite, troctolite, leucogabbro, leucogabbronorite, anorthosite; weakly layered to rhythmic; peridotite, dunite, wehrlite, harzburgite|
83318|Samphire Calcilutite|73213|6|Mentioned|959|||[?mistaken for Sandfire Calcilutite]|||||Mollusc-rich shelly carbonate mud.|
41467|San Sou Granite|50437|5|Briefly described|p5.6|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the San Sou Suite. Age: 1788 +/- 6Ma (SHRIMP). Used interchangeably with San Sou Monzogranite.||||||21-MAY-21
41467|San Sou Granite|66845|4|Described|p543, p544 Fig.10|||See San Sou Monzogranite. Three analysed grains (23, 6 and 18) ages of 3149, 2542 and 1809 Ma, reflect inheritance or crustal contamination.|magmatic age, 1788+/-6 Ma SHRIMP U-Pb|||||
31896|San Sou Suite|24197|5|Briefly described|p29|||Example of the Sybella Association. Geological Province: Kimberly region.||||||07-FEB-11
31896|San Sou Suite|50437|5|Briefly described|p1.6, 5.6, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1800Ma. Geological Province: Kimberley Region.||||||07-NOV-08
31896|San Sou Suite|71267|6|Mentioned|100k_interpgeop_lut.csv|||Geological province: Lamboo Province, Halls Creek Orogen. |||Includes San Sou Monzogranite.|||
39441|San Sou suite|22754|4|Described|p7|Paleoproterozoic|Paleoproterozoic|Age c. 1805-1790 Ma||||||07-NOV-08
39441|San Sou suite|66845|4|Described|p535, p536 Fig.2, p537 Fig.3, p539, p543|Paleoproterozoic|Paleoproterozoic|Contain youngest granites in Lamboo Complex and intrude Eastern and Central zones at southern end|1805-1790 Ma||Eastman Granite and San Sou Monzogranite||variably recrystallised, medium- to fine-grained leucocratic biotite monzogranite; high-K granites|
39441|San Sou suite|66846|6|Mentioned|p548 Fig. 1|||||||||
39441|San Sou suite|72437|5|Briefly described|p11, p110|Palaeoproterozoic|Palaeoproterozoic|Also intrudes basement rocks at the southern end of the Lamboo Complex. Consists of several small intrusions which are the youngest granitoids in the Lamboo Complex, but these are similar in age to the granitoids in the Granites-Tanami Inlier (Page and Sun, 1994).|c. 1790 Ma||Includes the San Sou Monzogranite and the Eastman Granite.|Intrudes the Halls Creek Group.||
32808|Sandy Creek Limestone|45038|14|Not recorded|p.78|||||||||
69034|Sans Sou Monzogranite|44231|5|Briefly described|Map Legend|||Medium- to fine-grained biotite monzogranite; scattered fine-grained mafic inclusions.||||||
36949|Santa Claus Member iron formation|23584|6|Mentioned|p14|||See Santa Claus Member. Geological Province: Yilgarn Craton.||||||
38616|Satarist Granite|23784|5|Briefly described|p21 Fig. 8|Archean|Archean|Age: c.2940 - 2930Ma.||||||07-NOV-08
38616|Satarist Granite|23936|5|Briefly described|Fig.4|Archean|Archean|Geological Province: Pilbara Craton. Age: ca. 2940-2930 Ma.||||||07-NOV-08
38616|Satarist Granite|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Age: ca. 2940-2930 Ma. Geological Province: Mallina basin||||||07-NOV-08
38616|Satarist Granite|24190|5|Briefly described|p820 Fig.1|Archean|Archean|Age: ca. 2940 - 2930 Ma||||||07-NOV-08
31915|Sater formation|43876|14|Not recorded|p561||Frasnian|||||||
39769|Satirist granitoid|24193|14|Not recorded|p874 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
77415|Saturn gabbro|65693|5|Briefly described|p7, p14.|||A concentrically-zoned elliptical pluton.|1072 +/- 8 Ma.||||Magnetite-rich olivine gabbro.|
77415|Saturn gabbro|67128|5|Briefly described|p5 Fig.4, p13, p25, p29|||Western Musgrave Province. Also appears as Saturn Gabbro on p13. An 11km long elliptical body. Geochemical resemblance to Alcurra Suite dykes. Age by Redstone Resources (written comm., 2007).|1072 +/- 8 Ma (baddeleyite).|Alcurra Suite.|||Comprises at least eight concentric rings of massive to weakly flow-banded olivine gabbro, typically containing oikocrysts of biotite and magnetite.|
77415|Saturn gabbro|68996|5|Briefly described|p7, p51, p52 tbl 7, p54, 67|Mesoproterozoic|Mesoproterozoic|Large igneous intrusion. See also Saturn intrusion p5, map p50, Saturn Gabbro p67.||Alcurra Dolerite|||Gabbro.|
77415|Saturn gabbro|69091|5|Briefly described|p136, p144|||A larger intrusion of Alcurra Dolerite.|1072 +/- 8 Ma|Alcurra Dolerite||Intrudes Tollu Group.||
23957|Savory Group|22589|4|Described|p123-6|Neoproterozoic||||||||
23957|Savory Group|22816|6|Mentioned|p15 Fig.7|||||||||
23957|Savory Group|22896|6|Mentioned|104|||||||||
23957|Savory Group|22907|6|Mentioned|39|||Obsolete name.||||||10-SEP-19
23957|Savory Group|23156|5|Briefly described|p12|Neoproterozoic|Neoproterozoic|The Savory Group occupies 85% of the Surface area of BULLEN.||||||
23957|Savory Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlain by Tarcunyah Group.||||||16-JUL-08
23957|Savory Group|23590|6|Mentioned|p14|||Now known as Disappointment Group? Now superseded.||||||
23957|Savory Group|23602|4|Described|p17|||Underlain by Tarcunyah Group.||||||16-JUL-08
23957|Savory Group|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Savory Basin.||||||
23957|Savory Group|23760|5|Briefly described|p25|||Superseded by Sunbeam Group. Geological Province: Officer Basin.||||||
23957|Savory Group|24017|6|Mentioned|p5 Tb. 1|||||||||
23957|Savory Group|24183|5|Briefly described|p5|||Contains the Calyie Formation, upper and the Diebel Subgroup||||||
23957|Savory Group|40888|6|Mentioned|p154|||||||||
23957|Savory Group|41669|3|Fully described|p49|||||||||
23957|Savory Group|41768|4|Described|p47|||||||||
23957|Savory Group|42278|6|Mentioned|p33|||||||||
23957|Savory Group|42704|5|Briefly described|Plate 2E||Neoproterozoic|Age: c.750Ma. Lithology is shale, siltstone, sandstone.||||||07-AUG-08
23957|Savory Group|42708|5|Briefly described|Plate 1|Proterozoic||||||||
23957|Savory Group|43055|5|Briefly described|p29|||||||||
23957|Savory Group|43056|5|Briefly described|Map Legend|||||||||
23957|Savory Group|43118|6|Mentioned|p16|||||||||
23957|Savory Group|43209|5|Briefly described|map legend||Neoproterozoic|||||||
23957|Savory Group|43229|5|Briefly described|Map Legend||Neoproterozoic|||||||
23957|Savory Group|43348|5|Briefly described|P8, Figure 1 p2|||Younger than Karara Formation||||||
23957|Savory Group|43756|4|Described|p533-542|||||||||
23957|Savory Group|43847|5|Briefly described|Map Legend||Proterozoic|||||||17-FEB-10
23957|Savory Group|43848|5|Briefly described|Map Legend||Proterozoic|||||||
23957|Savory Group|44111|6|Mentioned|p.55, p56 Fig.1, p61.|||in Savory Basin. Youngest components deformed by Paterson Orogeny. Partly coeval with Tarcunyah Group.||||||
23957|Savory Group|44139|5|Briefly described|p275, p277-279, p282|Neoproterozoic|Neoproterozoic|Newly recognized: Williams and Tyler (1989). Savory Basin. Unconformably overlies Yeneena Group. Includes the Calyie Sandstone. Contains a glacigene sequence similar to that in Amadeus Basin aged 750-690 Ma.| | ||||06-MAR-18
23957|Savory Group|44142|6|Mentioned|p309, p321-322, p324|||Savory Basin. New unit including the former Diebil Subgroup and eastern areas (Calyie Sandstone) of the Collier Subgroup (of the Bangemall Group).||||Unconformably overlies Manganese Subgroup (extensively faulted contact) and Cornelia Sandstone (surrounds the latter).||13-MAR-18
23957|Savory Group|61732|6|Mentioned|p84|||Superseded and subdivided in the northwestern Officer Basin area - several formations transferred to Mesoproterozoic (designation of units not clear). Geological Province: Savory Basin.||||||07-FEB-11
23957|Savory Group|62453|6|Mentioned|p52|||Geological Province: Officer Basin.||||||
23957|Savory Group|64777|5|Briefly described|p1|||Obsolete name.||||||
23957|Savory Group|64793|6|Mentioned|p283|||Former name; since been divided.||||||
23957|Savory Group|64943|6|Mentioned|p2, p17 Fig 10,19, 33,37|Neoproterozoic|Neoproterozoic|Shows faults and cleavage assigned to the Paterson Orogeny (Hickman and Bagas 1998), formed after 670 Ma (Williams 1992)||||||
23957|Savory Group|65102|6|Mentioned|p363, Figure 4-38, 364|Neoproterozoic|Neoproterozoic|Savory Basin. Glacial deposits considered coeval with Carnegie and Boord Formations, Amadeus Basin.||||||
23957|Savory Group|65403|5|Briefly described|p5, p14, p19, p28, p29.|||Basal part is correlative of Tarcunyah Group. Folded by the Blake Movement (between c.800 and 610 Ma).|900 - 610 Ma.||Includes Boondawari Formation.|Unconformably overlies Tarcunyah Group.||
23957|Savory Group|65404|6|Mentioned|p244, p245 Fig.1|Neoproterozoic|Neoproterozoic|||||||
23957|Savory Group|65416|6|Mentioned|p137.|Late Proterozoic|Late Proterozoic|Officer Basin.||||||
23957|Savory Group|65826|6|Mentioned|p7, p10. |||Term used by Williams (1992) for rocks in the Savory Basin, formerly the eastern part of the 'Bangemall Basin'; the names Savory Group and Savory Basin were abandoned: the lower part of the Group became the Sunbeam Group, and the upper part became the Disappointment Group (Bagas et al. 1999). Correlated with Tarcunyah Group in the Officer Basin.||||||
23957|Savory Group|71169|5|Briefly described|p81|Neoproterozoic|Neoproterozoic|||||||
37088|Savory Group""|23730|5|Briefly described|p6|||Replaced by Disappointment Group. Geological Province: Savory Basin.||||||
37088|Savory Group""|24017|6|Mentioned|p27|||||||||
37088|Savory Group""|50008|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Tillite. Age: c. 900 Ma.||||||
37088|Savory Group""|50188|5|Briefly described|p15|||Consisted of the former Diebil Subgroup and upper Collier Subgroup; but now comprises mostly Sunbeam and Disappointment Groups. Name no longer in use.||||||16-JUL-08
37088|Savory Group""|50228|6|Mentioned|p488|||Former name for rocks in the northwestern margin of the Officer Basin (no current name given).||||||
37088|Savory Group""|61732|6|Mentioned|p84|||Informal - see Savory Group.||||||07-FEB-11
70715|Savory Group''|62453|6|Mentioned|p52 |||Informal Name||||||
34438|Savory Group, lower|22716|6|Mentioned|table4, p230|Cryogenian|Cryogenian|Age: 830 Ma||||||
69964|Savory Group, lower""|49895|5|Briefly described|p12 Tb.1|Neoproterozoic|Neoproterozoic|Superseded by Sunbeam Group. Geological Province: Officer Basin.||||||
69965|Savory Group, upper""|49895|5|Briefly described|p12 Tb.1|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Superseded by the Disappointment Group.||||||
29959|Savoury Group|43055|5|Briefly described|Table 4|||Misspelling of Savory Group||||||
29959|Savoury Group|43862|6|Mentioned|p376|||Misspelling of Savory Group||||||
29959|Savoury Group|43868|6|Mentioned|p153|||Misspelling of Savory Group||||||
34602|Savoy Group|22816|6|Mentioned|p8 Table 1|||||||||
77237|Scamp Group|67375|6|Mentioned|p7 Fig.4, p16 Fig.10. |||Talbot Sub-basin, Musgrave Region.||||||
77237|Scamp Group|67553|6|Mentioned|p8,17,59|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin.||||||
77237|Scamp Group|69003|6|Mentioned|p37|Mesoproterozoic|Mesoproterozoic|Talbot Sub-basin, west Musgrave Province.||||||
77237|Scamp Group|71170|5|Briefly described|p5|||Talbot Sub-basin. Emplaced during the Giles Event.||||||
77237|Scamp Group|71211|6|Mentioned|p219|||Obsolete name, replaced by the Scamp Formation of the Mount Palgrave Group. ||||||
79626|Scamp granite|68996|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|[Informal, invalid name]||Scamp Formation|||Unit with granofelsic texture.|
77238|Scamp rhyolite|67375|6|Mentioned|p38 Table 1, p39, p46.|||An informal term used in this study for extrusive rhyolitic volcanic rocks (the Scamp volcanic association of Daniels, 1974) and intrusive granitic rocks, in the northwest Talbot Sub-basin. May be a component of the Mount Palgrave Group.||||||
77238|Scamp rhyolite|67553|5|Briefly described|p41-42,46,48|||Geological province: Musgrave Province, North Australian Craton. Informally known, equivalent to Scamp volcanic association of Daniel 1974. Significant similarities in age and composition to Mount Palgrave Group may indicate that this is a component of MPG (Howard er al., 2011). Outcrops to the north of Mount Waugh rhyolite.|||||Extrusive rhyolitic volcanic rocks; leucocratic rhyolitic rocks with slightly coarse crystalline groundmass.|
77238|Scamp rhyolite|69003|6|Mentioned|p52||||1064 +/- 5 Ma.|||||
35901|Scamp volcanic association|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Bentley Supergroup.||||||15-DEC-08
35901|Scamp volcanic association|44109|5|Briefly described|p117, p163|||Informal name. Of the Bentley Supergroup. Mainly felsic volcanics.||||||
35901|Scamp volcanic association|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Rhyolitic volcanic and volcaniclastic rock; metamorphosed.||||||15-DEC-08
35901|Scamp volcanic association|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Warakurna Supersuite|||Rhyolitic volcanic and volcaniclastic rock; metamorphosed|
35901|Scamp volcanic association|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite, basalt, volcanic breccia, rhyolite|
83324|Schist Hills Iron member|73089|6|Mentioned|p24, p26|||[Written as SHIM beds on p26]. Informal. Abbreviated to SHIM.||Callie Member, Dead Bullock Formation, Tanami Group||May be overlain by Killi Killi Formation.||
40823|Scorpion 'Subgroup'|50188|6|Mentioned|p9|||Superseded by Scorpion Group. Informal name format.||||||16-JUL-08
83390|Scotia Granite|73391|5|Briefly described|p26|||Split Rock.|2657 +/- 5 Ma.||||Granodiorite.|
39888|Scotia Granodiorite|24596|6|Mentioned|p561|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
37933|Scotia-Kanowna granite|24305|6|Mentioned|p924|||Not intended as a formal stratigraphic name.||||||
83939|Scotia-Kanowna monzogranite|70482|6|Mentioned|p317|Neoarchean|Neoarchean|Ross et al. (2004). Constitutes the bulk of the Scotia-Kanowna Dome, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.|2657 +/- 5 Ma (Ross, 2002).||||High-Ca type granite of tonalite-trondhjemite-granodiorite affinity.|
38793|Scotty Creek Conglomerate|23926|5|Briefly described|p28|||Geological Province: Yilgarn Craton.||||||
38793|Scotty Creek Conglomerate|24196|5|Briefly described|p47 Fig.5|Archean|Archean|Age: <2664 +/- 5 ma. Geological Province: Agnew-Mount Clifford Domain, Yilgarn Craton.||||||07-NOV-08
38793|Scotty Creek Conglomerate|64633|6|Mentioned|p6 Fig.4.|||Kurnalpi Terrane.|<2665 +/- 5 Ma (Krapez et al. 2000).|||||
40777|Scotty Creek Formation""|24494|6|Mentioned|p13|||Local name for the Jones Creek Conglomerate.||||||
80127|Scotty Creek Metasediments|71212|4|Described|intro p2, p1, p2, p13, p46, p53|Neoarchean|Neoarchean|Yilgarn Craton. Informal equivalent of the Scotty Creek Formation. Contains more than 75 percent of the gold mineralisation of the Lawlers region within secondary shears and vein stockworks. Deposited in a braided fluvial environment. Probably a lateral equivalent of the Jones Creek Conglomerate.  See also p54, p55, p60, p61-p63, p66, p69, p70, p73, p87-p94. p96, p97, p101-p103,p140, p143, p164, p171, p178, p190, p205, p235, p239, p240, p243, p246, p247, p250, p252, p258, p260, p261, App.B, App.D.||||Unconformably overlies the Agnew Komatiite and the Lawlers greenstones. Disconformably overlies the Vivien Metasediments. Overlain by the Waroonga Gneiss.|Coarse to fine-grained, variably pebbly, quartzofeldspathic sandstones and siltstones, rhyolitic porphyry and volcanics; some conglomerates and discontinuous lenses of serpentinite and amphibolite are also present.|
81589|Scotty Creek Sandstone|72057|5|Briefly described|p244|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Jones Creek Formation? or equivalent to?.||Overlain by Redeemer Dolerite.||03-SEP-19
77540|Scotty Creek Sequence|66880|6|Mentioned|p8, p10. |Archean|Archean|Fluvial deposits.||||||
77540|Scotty Creek Sequence|73151|6|Mentioned|p2|||Equivalent to the Scotty Creek Formation?||||||
77557|Scotty Creek Supersequence|66936|5|Briefly described|p137. |Archean|Archean|Northern Kalgoorlie Terrane. Interpreted to be time-equivalent of Kurrawang Supersequence. Deposition in shallow, sandy rivers.|||||Sandstones, quartzosericitic, medium- to coarse-grained, planar- to trough cross-bedded; lesser plane-laminated siltstone; basal cobble conglomerate and chloritic sandstone.|
77557|Scotty Creek Supersequence|66938|6|Mentioned|p187. |Archean|Archean|An axial (fluvial environment) system, with transport to the south or southeast, implying north to south paleoslopes. Depositional facies are characterisitic of high-discharge bedload draining areas of high relief.||||||
37896|Scotty Creek conglomerate|24135|6|Mentioned|p18|||Informal name.||||||
37896|Scotty Creek conglomerate|24196|5|Briefly described|p40|Archean|Archean|Age: 2664 +/- 5 Ma (Dunphy et al., in prep)||||||07-NOV-08
37896|Scotty Creek conglomerate|60416|6|Mentioned|p5|||Informal name.||||||
41130|Scotty Creek formation|24196|6|Mentioned|p68|||Informal. Now part of the Jones Creek Conglomerate. Geological Province: West Agnew-Mount Clifford sub-domain.||||||
40548|Scuddles Formation|23955|4|Described|p1239, p1242 Fig.3|||Overlies the Golden Grove Formation. Maximum Thickness: 990m. Geological Province: Murchison province, Yilgarn Craton.||||||
40548|Scuddles Formation|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Minjar Group.||||
40548|Scuddles Formation|69584|5|Briefly described|p5 Fig.2|Mesoarchean|Mesoarchean|Overlain by an unnamed formation of quartzite, banded iron formation and tholeiitic basalt.||Minjar Group||Overlies the Golden Grove Formation|Andesitic volcanics.|
40548|Scuddles Formation|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Minjar Group.||||
40548|Scuddles Formation|70020|4|Described|p128,131|||Geological province: Yilgarn Craton. Thickness: 730-990m.||Unit of Gossan Hill Group.|Includes Scuddles Formation Member 2.|Overlain by Cattle Well Formation. Underlain by Golden Grove Formation.|Quartz-feldspar phyric rhyodacite overlainand intruded by feldspar-quartz phyric dacite|16-JUL-19
40548|Scuddles Formation|70270|4|Described|p519-521, p523, 525, p528-529, p535-538|||Murchison Province.730-990m thick. Divided in to 4 informal members.||Of Gossan Hill Group||Contact with underlying Golden Grove Formation conformable to unconformable (erosional base).|Dacite volcanics, minor rhyodacite volcanics, volcanic breccia facies and sedimentary rocks.|
40548|Scuddles Formation|71168|4|Described|p11, p12 fig 6|||Yilgarn Craton. Appears as the Scuddles formation on p11. Thickness ranges from 730 to 990m. See also p13 fig 7, p50 fig 29, p57.||Gossan Hill Group||Overlies the Golden Grove Formation and is overlain by the Cattle Well Formation.|Quartz-feldspar-phyric dacite, minor rhyodacite volcanics and sedimentary rocks.|
34796|Scuddles Unit|22774|5|Briefly described|p572, Fig.2 p573|||See also Fig.3 p574, p573||||||
36854|Seabrook Sill|23582|5|Briefly described|Map Legend|Archean|Archean|Gabbro with pyroxenite; pyroxenite; peridotite - metamorphosed.||||||07-NOV-08
81729|Seven Mile Sandstone|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma; Yilgarn Craton events (4000 - 2600 Ma).|2657-2640 Ma (inferred)|Unit of Kurrawang Formation.|||Quartz-rich sandstone; massive to planar bedded; rare pebbly sandstone; rare cross-bedding; metamorphosed|
40549|Shadow Well Formation|23955|4|Described|p1241 Fig.2, p1242 Fig.3|||Overlain by the Gossan Valley Formation. Maximum Thickness: 1100m. Geological Province: Murchison province, Yilgarn Craton.||||||
40549|Shadow Well Formation|70020|4|Described|p131|||Geological province: Yilgarn Craton. Thickness: 150-1100m.||Unit of Gossan Hill Group.||Overlain by Gossan Valley Formation. Underlain unconformably by Murchison Monzogranite.|Quartz-feldspathic sandstone.|
40549|Shadow Well Formation|70270|5|Briefly described|p519 Fig. 2, p520 Fig. 3|||After Clifford, 1992 PhD. Murchison Province. 150-1100m thick.||Of Gossan Hill Group||Shown as unconformably overlying Murchison Monzogranite. Shown as overlain by the Gossan Valley Formation.|Quartz-feldspathic sandstone.|29-JUN-18
40549|Shadow Well Formation|71168|4|Described|p11, p12 fig 6, p13 fig 7|||Yilgarn Craton. Appears as the Shadow Well formation p11. Thickness ranges from 150 to 1100m.||Gossan Hill Group||Overlain by the Gossan Valley Formation. Intruded by the Murchison Monzogranite.|Quartz-feldspathic sandstone.|
34799|Shadow Well Unit|22774|5|Briefly described|p572, Fig.2 p573|||See also Fig.3 p574||||||
23962|Shag Pool Formation|41669|6|Mentioned|p36|||||||||
23962|Shag Pool Formation|43055|6|Mentioned|p21|||refers to informal usage of Davis (1977).||||||
72903|Shaw Granitic Complex|62576|6|Mentioned|p619, p629|||||||||
72903|Shaw Granitic Complex|63441|6|Mentioned|p30|Archean|Archean|Structural term. Includes the Tambina and Cutinduna Supersuites.||||||07-FEB-11
72903|Shaw Granitic Complex|64405|5|Briefly described|p2 Fig. 1|||||||||07-FEB-11
72903|Shaw Granitic Complex|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Granitic rock; metamorphosed.||||||15-DEC-08
72903|Shaw Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
72903|Shaw Granitic Complex|65827|6|Mentioned|p15|||Granitic components contain inherited 3650-3550 Ma zircons indicative of ancient sialic crust.
||||||
72903|Shaw Granitic Complex|66217|5|Briefly described|p8, p24, p44.|Paleoarchean|Paleoarchean||||Includes North Shaw Suite and rocks of the Callina Supersuite.|Is overlain unconformably by Fortescue Group (Mount Bruce Supergroup).||
72903|Shaw Granitic Complex|67197|6|Mentioned|p3|||East Pilbara Terrane.||||||
72903|Shaw Granitic Complex|67270|6|Mentioned|p3|Archean|Archean|||||||
72903|Shaw Granitic Complex|68035|5|Briefly described|p287, 284 Fig 1|Paleoarchean|Paleoarchean|Xenoliths of 3.58 Ga gabbroic anorthosite (McNaughton et al., 1988) occur within 3.43 Ga granitic rocks.||||||
72903|Shaw Granitic Complex|69301|6|Mentioned|p5 Fig.3, p11|||On western margin of Shaw Granitic Complex, xenoliths of 3.58 Ga gabbroic anorthosite have been reported within ca 3.43 Ga granitic rocks.||||||
72903|Shaw Granitic Complex|70022|6|Mentioned|p114, 121|||East Pilbara Terrane. Contains ~3.58 Ga meta-anorthosite pods; possible fragments of Pilbara Craton substrate.||||||
72903|Shaw Granitic Complex|70733|6|Mentioned|p105|||Eastern Pilbara Craton.||||||
72903|Shaw Granitic Complex|73598|6|Mentioned|p1208 Fig.1|||East Pilbara Terrane. Appears as Shaw Granite Complex.||||||
33448|Shaw Granitoid Complex|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 2850 Ma||||||07-NOV-08
33448|Shaw Granitoid Complex|22475|6|Mentioned|p493|||||||||
33448|Shaw Granitoid Complex|22906|5|Briefly described|p46, p48 Fig. 4|Archean|Archean|Includes tonalite gneisses dated to c.3.45Ga (Bickle et al, 1993).  Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|23416|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton||||||07-NOV-08
33448|Shaw Granitoid Complex|23755|4|Described|p48|Archean|Archean|Age: 3417+/-40 Ma (U-Pb zircon).||||||07-NOV-08
33448|Shaw Granitoid Complex|23780|5|Briefly described|p38|Archean|Archean|Age: ~3462+/-3 Ma||||||07-NOV-08
33448|Shaw Granitoid Complex|23783|5|Briefly described|p17|Archean|Archean|||||||07-NOV-08
33448|Shaw Granitoid Complex|23807|6|Mentioned|p108|||Geological Province: Pilbara Craton.||||||
33448|Shaw Granitoid Complex|23813|6|Mentioned|p117|||||||||
33448|Shaw Granitoid Complex|23895|5|Briefly described|p883, p884 Fig.1|Archean|Archean|Referred to as SGC throughout text. Of the East Pilbara Granite-Greenstone Terrain.||||||07-NOV-08
33448|Shaw Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3459-2851Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33448|Shaw Granitoid Complex|24184|4|Described|p703, 706|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3490-3410Ma||||||07-NOV-08
33448|Shaw Granitoid Complex|24185|5|Briefly described|p751|Archean|Archean|Age: ca. 3475-3400 Ma (Van Kranendonk and Hickman, 2000). Geological Provice: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|24193|5|Briefly described|p889 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|24531|4|Described|p25, p8-9 Fig. 3|Archean|Archean|Age: c.3578Ma.  See also p2, p5.||||||07-NOV-08
33448|Shaw Granitoid Complex|24532|5|Briefly described|Map legend|Archean|Archean|Of the Pilbara Supergroup.  Age: ~2850Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|24550|6|Mentioned|p32, p33|Archean|Archean|Age: 2900-2840Ma.||||||07-FEB-11
33448|Shaw Granitoid Complex|24590|5|Briefly described|p29, p31|Archean|Archean|Contains enclaves of 3578+/-4Ma anorthosite and gabbro.||||||07-FEB-11
33448|Shaw Granitoid Complex|44150|5|Briefly described|p129, p130-131 Fig.2-130, p133, p142|||See also p143 Tb.2-21, p148 Fig.2-136, p151-156, p158. Covers 3300 sq km.|3.5 Ga.||Includes North Shaw Tonalite; Spear Hill, Cooglegong, Coondina, Eley, Bamboo Springs and Mulgandinnah Adamellites.||Biotite monzogranites, tonalite, granodiorite, migmatite, gneiss, greenstones.|
33448|Shaw Granitoid Complex|50381|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|50423|4|Described|p216, 217||Archean|Southern margin unconformably overlain by Fortescue Group. Intrudes greenstones to N. Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|50427|5|Briefly described|p182 Fig.5|Archean|Archean|Seven principal components, including amphibolite-granulite facies, tonalite, granodiorite, migmatised orthogneiss, mafic diorite, leucogranite, granite and monzogranite.||||||07-NOV-08
33448|Shaw Granitoid Complex|61111|6|Mentioned|p96 Fig.2|||||||||
33448|Shaw Granitoid Complex|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Structural term. Geological Province: Pilbara Craton.||||||07-NOV-08
33448|Shaw Granitoid Complex|64326|6|Mentioned|p71 Fig. 1|Archean|Archean|Geological province: Hamersley Basin/Marble Bar Sub-basin.||||||07-FEB-11
33448|Shaw Granitoid Complex|64747|6|Mentioned|p94 fig 1|||||||||
33448|Shaw Granitoid Complex|69167|6|Mentioned|178044.1.pdf|||Age derived from biotite monzogranite sample (178049.1.pdf)|2926 +/- 6 Ma (SHRIMP)|||||
32599|Shaw River granite|45923|14|Not recorded|p.49,94||Paleoproterozoic|L.Prot?||||||07-NOV-08
39770|Shaw granitoid complex|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton. Informal name - see Shaw Granitoid Complex.||||||07-NOV-08
78518|Shay Cart monzogranite|68107|6|Mentioned|p617|Neoarchean|Neoarchean|NE Yilgarn craton.|2634 Ma (Wingate et al. 2011).|||||22-SEP-14
69193|Shed Well formation|60629|6|Mentioned|p96 Fig.2|||Informal.||||||
30591|Shepherds Bore Plutonic Complex|23621|2|Defined|p56 Appendix|Statherian|Orosirian|See also page 20, 10 table 1. Age: ~1843-1790 Ma. Of Sally Downs supersuite. Overlying unit King Leopold Sandstone (unconformably). Geological Province: Bow River Batholith.||||||
30591|Shepherds Bore Plutonic Complex|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Bow River Batholith.||||||07-NOV-08
30591|Shepherds Bore Plutonic Complex|24173|3|Fully described|p21, p12 Tb.2|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs supersuite. Overlain by King Leopold Sandstone. Geological Province: Halls Creek Orogen. Previously mapped as Bow River Granite and McIntosh Gabbro. Intrudes the Koongie Park Formation. Age: <1835Ma||||||07-NOV-08
30591|Shepherds Bore Plutonic Complex|50437|6|Mentioned|p4.1|||Of the Syenite Camp Suite (Sally Downs Supersuite). Geological Province: Kimberley Region.||||||
28999|Sholl Creek Formation""|31217|6|Mentioned|p42|||refs. Hall and Goode (1975).||||||
73593|Sholl Intrusion|63441|5|Briefly described|p12 Tb. 2|Archean|Archean|Of the Radley Suite. Contains nickel-copper deposits. Geological Province: West Pilbara Superterrane - named for Mount Sholl. Also referred to as Mount Sholl layered intrusion (p38).||||||07-FEB-11
73593|Sholl Intrusion|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbro, anorthosite, peridotite, ultramafic schist|
34384|Sholl succession|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3150-3100Ma.||||||07-NOV-08
29000|Siberia Complex|38474|4|Described|p1776|||||||||
38583|Siberia Komatiitic Volcanics|23782|5|Briefly described|p9|||Geological Province: Yilgarn Craton.||||||
38583|Siberia Komatiitic Volcanics|68289|6|Mentioned|p27|||Referred to as the Siberia Komatiite volcanics on p27.||||Overlies the Walter Williams Formation.||
39256|Siberia komatiite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Ora banda Domain.  Of the Linger and Die Group.  Age: 2708 +/- 7Ma.||||||07-NOV-08
39256|Siberia komatiite|24229|6|Mentioned|p161, p162 Fig.2|||Informal name.||||||
40287|Silver Lake Member, lower|24322|5|Briefly described|p58|Archean|Archean|Informal.  Of the Kambalda Komatiite Formation.  Of the Kambalda Group.||||||07-NOV-08
40288|Silver Lake Peridotite member|24322|5|Briefly described|p62|Archean|Archean|Informal.  Of the Kambalda Komatiite Formation.  Of the Kambalda Group.||||||07-NOV-08
23974|Singleton Basalt|42533|3|Fully described|p83|||Name reserved.||||||
23974|Singleton Basalt|44149|5|Briefly described|p33 fig 2-29, p35 fig 2-30, p41|Archean|Archean|See also p43 Fig.2-44, p47-48. Of Murchison Province. 1km thick. Lower portion thought to be remnants of a shield volcano; upper portions, of stratovolcanoes.||Mount Farmer Group|||Basal 1 km sequence of ultramafic rock, gabbro, high-Mg basalt, and BIF; overlain by a 2.5 km sequence of massive and pillowed tholeiites; then pillowed and pyroclastic tholeiites. Abundant subvolcanic gabbro and dolerite sills, some layered.|
23974|Singleton Basalt|65268|6|Mentioned|p6 fig 4, p5 fig 3|||||Unit in Mount Farmer Group.|||Tholeiitic basalt; mafic pyroclastic rocks; high-Mg basalt with ultramafic rocks.|
23974|Singleton Basalt|69267|6|Mentioned|p654|||Murchison Province, Yilgarn Craton.||Mount Farmer Group.||||
78992|Singleton Basalt Member|70226|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Carton. 10 facies are mapped separately.||Yalgoo Formation|||Basalt (locally spherulitic, variolitic, pillowed or amygdaloidal); pyroxene spinifex-textured basalt; hyaloclastite; glassy basaltic andesite flows; all metamorphosed. Also, psammite, rare peperite; interlayered mafic/ultramafic schist.|16-DEC-15
78992|Singleton Basalt Member|70796|5|Briefly described|100k_geologyl_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton, Youanmi Terrane. See also 100k_geologyp_lut.csv, 100k_interpgeol_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, Yalgoo100_2241_stratig.pdf. Numerous additional lithologies are discussed.|2793 +/ 8 Ma (isotopic)|Yalgoo Formation|||Basalt, psammite horizons, locally well bedded and crossbedded; rare peperitic contacts with lava flows. Mafic schist with minor ultramafic schist and metabasalt; Interlayered pillow lava and hyaloclastite.|
78992|Singleton Basalt Member|70830|5|Briefly described|p57|||Murchison Domain.|c. 2795 Ma|Yalgoo Formation.|||Basaltic pillow lava and fragmental mafic volcaniclastic rocks, locally abundant volcaniclastic siltstone and sandstone.|
78992|Singleton Basalt Member|71269|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3131-2600 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv.|2793-2760 Ma|Unit of Yalgoo Formation.|||Basalt: pyroxene spinifex-textured; amygaloidal, pillowed, spherulitic, massive, weakly pillowed, minor andesite flow, metamorphosed; mafic to minor ultramafic schist; actinolite-tremolite-chlorite; locally sheared; pillow lava and hyaloclastite|
74720|Sir Fredrick Conglomerate|64580|4|Described|map legend||Neoproterozoic|Conglomerate.||||||15-DEC-08
32220|Six Mile Creek Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Sulphur Springs Group, Pilbara Craton||||||07-NOV-08
32220|Six Mile Creek Formation|23755|4|Described|p36|Archean|Archean|See also page 17 table 1.  Of Sulphur Springs Group.||||||07-NOV-08
32220|Six Mile Creek Formation|23783|5|Briefly described|p16|||of Euro Basalt - formerly part of Sulphur Springs Group.||||||
32220|Six Mile Creek Formation|23891|5|Briefly described|p90|Archean|Archean|Basal unit of Sulphur Springs Group. Geological Province: Pilbara Craton.||||||07-NOV-08
32220|Six Mile Creek Formation|23956|5|Briefly described|p1264|||Of the Sulphur Springs Group. Geological Province: Pilbara Craton.||||||
32220|Six Mile Creek Formation|24184|5|Briefly described|p702|Archean|Archean|Overlying Unit: Leilira Formation. Geological Province: Pilbara Craton. Formerly the lowermost unit of the Sulphur Springs Group, now reassigned to underlying Euro Basalt||||||07-NOV-08
32220|Six Mile Creek Formation|24531|5|Briefly described|p18|Archean|Archean|Previously the base of the Sulphur Springs Group, this unit is now redefined as the unconformity at the base of the Leilira Formation.||||||07-NOV-08
32220|Six Mile Creek Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Sulphur Springs Group. Mafic volcanic rocks, minor volcaniclastic rocks.||||||07-FEB-11
32220|Six Mile Creek Formation|61253|5|Briefly described| p51|Archean|Archean|Formerly included at the base of Sulphur Springs Group.  Due to chemical silimarities it is now considered to be part of Euro Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
32220|Six Mile Creek Formation|61266|4|Described|p58 Tb.1, p59|Archean|Archean|Of the Sulphur Springs Group. Overlain by the Leilira Formation. Mafic volcanic rocks, minor volcaniclastic rocks. Max. thickness: 2200m. Geological Province: Pilbara Craton.||||||07-NOV-08
32220|Six Mile Creek Formation|63441|5|Briefly described|p6 Tb. 1, p21|Archean|Archean|Obsolete name. Of Van Kranendonk and Morant (1998). Formerly within Sulphur Springs Group. Now reinterpreted to be part of the unconformably underlying Euro Basalt, based on map and geochemical data.||||||07-FEB-11
79793|Sixty-six Hill Member|68574|6|Mentioned|p3|||||Lizard Hills Formation.||||
79423|Sixty-six Hills Member""|67201|5|Briefly described|p20|||Informally named unit. May represent Farrel Quartzite in west Pilbara. Refers to lenticular units of sandstone and conglomerate that locally underlie Cleaverville Formation (Gorge Creek Group, Gorge Creek Basin) and unconformably overlie Regal Formation (Regal Terrane), at Cleaverville (Kiyokawa and Taira, 1998). See Farrel Quartzite.||||In west Pilbara, is overlain by Cleaverville Formation and overlies Regal Formation.|Lenticular units of sandstone and conglomerate.|25-NOV-16
36034|Skirmish Hill Volcanic Association|30942|6|Mentioned|Map legend||Mesoproterozoic|Informal unit used in Proterozoic Granites GIS. Desc: Porphyritic acid volcanic rocks. Minor basic volcanics.||||||
41371|Skirmish Hill Volcanics|24496|5|Briefly described|p21 Tb.2|Mesoproterozoic|Mesoproterozoic|Interpreted as caldera complexes. Of Bentley Supergroup. Geological Province: Musgrave Block.||||||04-FEB-05
41371|Skirmish Hill Volcanics|50607|5|Briefly described|p3.2|||Geological Province: Musgrave Block. Of the Bentley Supergroup.||||||
41371|Skirmish Hill Volcanics|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Interpreted as Caldera Complex. Of Bentley Supergroup. Geological Province: Musgrave Block.||||||22-FEB-05
41371|Skirmish Hill Volcanics|65135|5|Briefly described|p6 Fig.4, p14, p16|Stenian|Stenian|Of Warakurna Supersuite. Felsic-dominated bimodal volcanic sequence in the far western Musgrave Complex. Dated at 1076 +/- 6 Ma. Possibly the surface expression of ~1075 Ma intrusions to the north. Possible equivalent of Puntitjata Rhyolite.||||||
41371|Skirmish Hill Volcanics|65693|6|Mentioned|p3 Fig.1.|||||||||
41371|Skirmish Hill Volcanics|65833|4|Described|p6 Fig.4, p14, p16|Stenian|Stenian|Of Warakurna Supersuite. Felsic-dominated bimodal volcanic sequence in the far south of the Musgrave Complex. 1076 +/- 6 Ma (GSWA). Possibly the surface expression of c.1075 Ma intrusions further north.||||||
41371|Skirmish Hill Volcanics|67128|5|Briefly described|p5 Fig.3, p27, p30|||Occurs in the far south of the western Musgrave Province. Age equivalent of Puntitjata Rhyolite.|1078 +/- 4 Ma.|Bentley Supergroup.|||A felsic-dominated bimodal volcanic sequence; not strongly deformed.|
41371|Skirmish Hill Volcanics|68996|5|Briefly described|p7, p52 tbl 7, p57, 62, 64|Mesoproterozoic|Mesoproterozoic|See also map p50.|1078+/-4 Ma U/Pb SHRIMP|Kunmarnara Group|||Rhyolites to dacites.|
70173|Skirmish Hill volcanic association|44109|5|Briefly described|p117|Mesoproterozoic|Mesoproterozoic|Informal name. Of the Bentley Supergroup. Mainly felsic volcanics.||||||
70173|Skirmish Hill volcanic association|64580|4|Described|map legend||Mesoproterozoic|Of Warakurna Supersuite. Rhyolitic volcanic and volcaniclastic rock; minor basalt; metamorphosed.||||||15-DEC-08
70173|Skirmish Hill volcanic association|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1075 Ma.|Unit in Bentley Supergroup.|||Andesite, dacite, rhyodacite, granophyre.|
70173|Skirmish Hill volcanic association|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1075 Ma.|Unit in Bentley Supergroup.|||Rhyodacite and dacite; plagioclase phenocrysts and glomerophenocrysts up to 8 mm; locally amygdaloidal; includes layers or sheets of medium-grained granophyre.|
70173|Skirmish Hill volcanic association|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Warakurna Supersuite|||Rhyolitic volcanic and volcaniclastic rock; minor basalt; metamorphosed|
34157|Sloansville Subgroup|22642|6|Mentioned|485|||Indexing misspelling of Soansville Subgroup, which is a misspelling of Soanesville Subgroup. Geol province Pilbara Craton||||||
33867|Smithfield Ultramafics""|22534|6|Mentioned|p9|||Superseded by Highway Ultramafics||||||
75373|Smoke Hill Felsic Volcanic|64745|5|Briefly described|p376|Stenian|Stenian|Probable misspelling. Paper implies of Tjauwata Supercrustals. Age: ca. 1.075Ga.||||||18-SEP-09
75373|Smoke Hill Felsic Volcanic|71211|6|Mentioned|p234|||Smoke Hill Volcanics also used p233.|ca. 1075 Ma|Tjauwata Group||||
41372|Smoke Hill volcanics|24197|5|Briefly described|p97|||Informal - see Smoke Hill Volcanics. Of the Tollu Group (Bentley Supergroup). Age: 1080Ma. Geological province: Musgrave Complex.||||||07-FEB-11
41372|Smoke Hill volcanics|50607|5|Briefly described|p1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Of the Tollu Group/Winburn Suite.  Age: 1080Ma.||||||
73850|Snapper Beach Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Cleaverville Group. Felsic volcanics, black-white chert, felsic tuff, ferruginous chert and banded iron formation. Overlies Dixon Pillow Basalt. Geological Province: Pilbara Block.||||||07-NOV-08
73850|Snapper Beach Formation|68574|6|Mentioned|p4|||Kiyokawa and Taira (1998); formerly Cleaverville Formation (Ryan and Kriewaldt, 1964; Hickman, 1997), included in their Cleaverville Group. Both names abandoned: there is no official Snapper Beach in the area.||||||
72549|Snot Rocks monzogranite|62107|6|Mentioned|p1391 Fig. 2|||Informal name. In the Eastern Goldfields Province.||||||
81382|Songvang Basalt|70326|3|Fully described|p334,336,338-9,341,343,346-51|Neoarchean|Neoarchean|Geological province: Agnew region, Ora Banda Domain, Kalgoorlie Terrane, Yilgarn Craton. Extrusive subaqueous lava sheet flows intruded by a comagmatic layered mafic sill att he base. Compositionally, the Songvang Basalt is a komatiitic basalt with pronounced LREE enrichment. Thickness: ~335m. Observed in several drillholes on the Agnew Anticline western limb, and sporodically in outcrop. Major and trace element geochemical analysis on Table 4 p342-346. Evidence of crustal contamination e.g. negative Nb and T ianomalies; [La/Sm]PM> 1; Pearce, 2008; van Hunen and Moyen, 2012). See also p353-4,360-1,363-5.||||Underlain by Hickies Bore Basalt. Correlable to Mount Keith Ultramafic.|Upper: Chl-altered porphyroclasts in a groundmass of Hbl, Qz and Fld. Lower: microspinifex texture, an altered groundmass mostly of Tlc, Srp and Opq. Includes one thin mudstone. Submarine sheet flows and comagmatic differentiated intrusion.|
81382|Songvang Basalt|73151|6|Mentioned|p10|||Yilgarn Craton. Kalgoorlie Terrane, Agnew Greenstone Belt.||||||
81382|Songvang Basalt|73596|6|Mentioned|p1151-1153, 1156-1157, 1161-1163, 1165|Neoarchean|Neoarchean|See also p1167. Lawlers Domain, Agnew-Wiluna Greenstone Belt. Deep-water mafic-ultramafic lava fields and feeder intrusions. Is intruded by a 2691 +/- 9 Ma orthogneiss precursor. Lateral facies equivalent of upper McFarlanes Basalt.||||Overlies Hickies Bore Basalt. Is overlain paraconformably by Mount Keith Dacite and Never Can Tell Basalt, and unconformably by Cosmos Volcanic Complex. See COMMENTS for more.||
37192|Sophie Downs "Granite"|23599|6|Mentioned|p7|||||||||
34454|Sophie Downs Granophyre|22754|5|Briefly described|p6, p8|Paleoproterozoic|Paleoproterozoic|Of Sophie Downs suite.  Age: c. 1920-1910 Ma||||||07-NOV-08
34454|Sophie Downs Granophyre|63866|5|Briefly described|p128|Orosirian|Orosirian|Eastern Zone, Halls Creek Orogen. Previously the Sophie Downs Granite.|c. 1912-1907 Ma|||||
32523|Sophie Downs Granophyre Member|23599|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of Ding Dong Downs Volcanics.||||||07-NOV-08
32523|Sophie Downs Granophyre Member|23621|2|Defined|p56 Appendix|Orosirian|Orosirian|See also page 14, 12 table 1. Previously named Sophie Downs Granite. Age: 1912+/-3 Ma (U-Pb zircon). Of Ding Dong Downs Volcanics. Overlying unit Saunders Creek Formation (unconformably). Halls Creek Orogen. Max. thickness: >1000 m.||||||
32523|Sophie Downs Granophyre Member|23622|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
32523|Sophie Downs Granophyre Member|24173|3|Fully described|p15|Paleoproterozoic|Paleoproterozoic|Of the Ding Dong Downs Volcanics. Unconformably overlain by Saunders Formation. Previously known as Sophie Downs Granite. Age: 1907 +/- 6Ma and 1912 +/- 3Ma. Intruded by Woodward Dolerite||||||07-NOV-08
32523|Sophie Downs Granophyre Member|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Ding Dong Downs Volcanics. Leucocratic porphyritic granophyre and leucogranite; metamorphosed.||||||15-DEC-08
32523|Sophie Downs Granophyre Member|69099|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Old name for Sophie Downs Granite?||Ding Dong Downs Volcanics|||Leucocratic porphyritic granophyre and leucogranite; metamorphosed.|04-AUG-15
32523|Sophie Downs Granophyre Member|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Ding Dong Downs Volcanics|||Leucocratic, porphyritic granophyre and leucogranite; metamorphosed.|
32523|Sophie Downs Granophyre Member|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Unit of Ding Dong Downs Volcanics.|||Leucocratic porphyritic granophyre and leucogranite; metamorphosed|
32523|Sophie Downs Granophyre Member|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Ding Dong Downs Volcanics.|||Leucocratic porphyritic granophyre and subordinate leucogranite, massive to schistose; minor amphibolite and biotite schist|
32523|Sophie Downs Granophyre Member|71397|4|Described|p8|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Nomenclature of Blake et al. (2000) to replace usage of "Sophie Downs Granite", and included the Ding Dong Downs Volcanics. Blake et al. (2000) justified this change to highlight the shallowintrusive nature of the felsic igneous rocks within the Sophie Downs Dome. However, in the absence of contact relationships, this Report uses the original nomenclature.||||||
39849|Sophie Downs Trachyte|22754|6|Mentioned|p20|||||||||
39849|Sophie Downs Trachyte|24572|6|Mentioned|Map - list|||Geological Province: Halls Creek Orogen.||||||
30661|Sophie Downs suite|22754|4|Described|p3, p6|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  Age: c.1910Ma.||||||07-NOV-08
30661|Sophie Downs suite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1913 +/- 5 Ma.||||||07-FEB-07
30661|Sophie Downs suite|72437|5|Briefly described|p7, p51|Palaeoproterozoic|Palaeoproterozoic|Previously thought to intrude the Halls Creek Group, however Griffin and Tyler (1992b) demonstrated an unconformity between these two units indicating this suite forms basement.|c. 1910 Ma||Includes the Sophie Downs Granite, Esaw Monzogranite, Junda Microgranite.|||
32610|South Grosmont Granite|46311|14|Not recorded|p.10|||||||||
78079|South Perth Shale Formation|68254|6|Mentioned|p1039, p1046 Tb.4-5|||See also South Perth Shale.||||||
70222|South Perth Shale, lower|24410|5|Briefly described|p28|Cretaceous|Cretaceous|Informal name. Of the Warnbro Group||||||
81163|South Perth formation|71790|6|Mentioned|p102|||Palynology p. 102.||||||
34539|Southern Cross Greenstone Belt|22775|6|Mentioned|5|||||||||
67875|Southern Cross greenstones|60076|5|Briefly described|p15|||Informal name for sequence of greenstones in S.Cross Province.  Quartz-pebble conglomerate at the base; basalts with interleaved komatiite and regionally persistent BIF units; with metasedimentary rocks and felsic volcanic complexes towards the top.||||||
40784|Southern Cross quartzites|50128|6|Mentioned|p43|||Informally referring to quartzites of the Southern Cross Granite-Greenstone Terrane. Geological Province: Yilgarn Craton.||||||
25487|Southern granite""|31044|6|Mentioned|p229|||||||||
41373|Southern granites|24197|6|Mentioned|p98|||Informal name for group of granites in the southern part of the Musgrave Block and which are thought to be part of the Kulgera Supersuite.||||||07-FEB-11
41373|Southern granites|50607|6|Mentioned|p2.2|||Geological Province: Musgrave Block. Of the Kulgera Supersuite.||||||
80943|Spargoville Sequence|70276|6|Mentioned|p783|||Kalgoorlie terrane, Yilgarn Craton.||Black Flag Group.|||Part of a complex felsic volcaniclastic succession.|
80943|Spargoville Sequence|72049|6|Mentioned|p256, p259-p260|||||||||
80943|Spargoville Sequence|73391|5|Briefly described|p50, 201, 217, 221, Appendices.|||Krapez et al. (2000).||Black Flag Beds.|Spargoville Formation.||Volcaniclastic and epiclastic turbidites, with intervening condensed sections of carbonaceous shales.|
41131|Spargoville formation|24196|6|Mentioned|p31|||||||||
67872|Spargoville pegmatite|60076|6|Mentioned|p37|||Informal name.  On YILMIA sheet.  Has yielded beryl, lepidolite, petelite and tantalite-columbite.||||||
30674|Spark Range Conglomerate|43281|6|Mentioned|Map legend|Late Devonian|Late Devonian|Canning Basin.||||||
31978|Sparke conglomerate|43876|14|Not recorded|p561|Famennian|Frasnian|||||||
25488|Spear Hill Adamellite|30485|6|Mentioned|p74|||Refers Hickman & Lipple (1974)||||||
25488|Spear Hill Adamellite|37633|5|Briefly described|Plate 4|||||||||
25488|Spear Hill Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
25488|Spear Hill Adamellite|39697|4|Described|p33|||||||||
25488|Spear Hill Adamellite|41349|6|Mentioned|p4|||||||||
25488|Spear Hill Adamellite|44150|5|Briefly described|p143 Tb.2-21, p148 Fig.2-136|||8 sq km area. Post-tectonic granitoid.||Shaw Granitoid Complex|||Biotite monzogranite; minor porphyritic and granophyric types. Intruded by rhyolite and dolerite dykes.|
25488|Spear Hill Adamellite|63441|5|Briefly described|p12 tb. 2|Archean|Archean|Superseded by Spear hill Monzogranite (Split Rock Supersuite).||||||07-FEB-11
70729|Spearhole Formation, upper|62453|6|Mentioned|p18|||Informal name.||||||
39287|Spearhole Sandstone|24246|6|Mentioned|p17|||Geological Province: Savory Basin.||||||
42404|Spearwood Dune System|23816|5|Briefly described|p255, 256|Late Pleistocene|Late Pleistocene|Geological Province: Perth Basin. Age: 26 800 +/- 1050 yrs B.P.||||||27-APR-05
42404|Spearwood Dune System|40400|6|Mentioned|p109|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
42404|Spearwood Dune System|63745|6|Mentioned|p59, p67|||See also p60 Fig. 1.||||||07-FEB-11
42404|Spearwood Dune System|69840|6|Mentioned|p183, p186 Fig.3|Pleistocene|Pleistocene|Synonymous with Tamala Limestone. Parallel to the coast this unit is the located between Quindalup Dune System and Bassendean Dune System.|||||Carbonate sand.|
42404|Spearwood Dune System|71780|14|Not recorded|Plate 2|||No white card.||||||
73389|Spearwood Dunes|60556|5|Briefly described|p21|||Informal.||||||13-NOV-07
73389|Spearwood Dunes|63330|5|Briefly described|p192, p193 Fig. 5, p200 Tb. 3|Quaternary|Quaternary|Large scale, linear, near-continuous subparallel ridges (up to ca.60m relief) with intervening narrow, steep-sided depressions, or of narrow plains. Overlie Pleistocene limestone blanketed by quartz sand. Equivalent is Yalgorup Plain.||||||
39848|Spearwood Sand|24464|5|Briefly described|p332 Fig. 1|||||||||
32964|Spearwood System""|44303|14|Not recorded|p.12|||(ref. to McArthur & Bettanay 1960). (I/50-5,9).||||||
29992|Spherule Marker Bed|24041|5|Briefly described|p495|Archean|Archean|Of Bee Gorge Member, Wittenoom Formation.  Age: 2548 +26/- 29Ma (Pb-Pb)  Geological Province: Pilbara Craton||||||07-NOV-08
29992|Spherule Marker Bed|43064|5|Briefly described|p69|||Informal stratigraphic unit of Bee Gorge Member.||||||
29992|Spherule Marker Bed|60706|6|Mentioned|p629 Fig. 4k, p633|Archean|Archean|Informal reference to layer of sperules within the Bee Gorge Member (Wittenoom Formation). Age: 2565+/-9 Ma (SHRIMP); also 2541+18/-15 Ma (Woodhead et al., 1998)||||||07-NOV-08
29992|Spherule Marker Bed|65757|5|Briefly described|p87, p87 Fig.7, p88|||Age 2565+/-9 Ma. Wittenoom Formation,?above Bee Gorge Member. Overlain by ferruginous shale. In the Hamersley Basin||||||
29992|Spherule Marker Bed|70733|6|Mentioned|p112, 116|||||Wittenoom Formation.||||
25490|Split Rock Formation|37373|6|Mentioned|p90|||||||||
25490|Split Rock Formation|44115|14|Not recorded|p17|||See also Lexicon.||||||
78324|Split Rock Suite|65008|6|Mentioned|p21|Mesoarchean|Mesoarchean|Misspelt, see Split Rock Supersuite in this paper. Van Kranendonk et al. (2004). Exhibits a pronounced radiometric signature.|c.2850 Ma.||||Tin granites.|15-MAY-14
72547|Split Rock granodiorite|70482|6|Mentioned|p317|Neoarchean|Neoarchean|Occurs in the centre of the Scotia-Kanowna Dome batholith, Eastern Goldfields Superterrane, Eastern Yilgarn Craton.|2657 +/- 5 Ma (Nelson, 1995).|||||
81569|Split rocks Supersuite|71550|6|Mentioned|p45|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton.|2.83-2.80 Ga|||||
38803|Spring Well Volcanic complex|23930|6|Mentioned|p128|Archean|Archean|Informal name - see Spring Well Complex. Geological Province: Yilgarn Craton.||||||07-NOV-08
29015|Spring Well complex|23591|5|Briefly described|p10|||See also page 8, 6 Fig. 3.  Geological Province: Yilgarn Craton.||||||
29015|Spring Well complex|23786|5|Briefly described|p24|||Informal name.  Geological Province: Yilgarn Craton.||||||
29015|Spring Well complex|24135|6|Mentioned|p17|||Informal - see Spring Well Complex.||||||
29015|Spring Well complex|24174|6|Mentioned|p23|||Informal name.  See also Spring Well felsic volcanic complex.||||||
29015|Spring Well complex|37793|6|Mentioned|Fig.1|||||||||
29015|Spring Well complex|38543|4|Described|p277|||||||||
29015|Spring Well complex|40770|6|Mentioned|p418|||||||||
37198|Spring Wells Complex|23611|5|Briefly described|p13|Archean|Archean|Age: 2690 +/- 6 Ma.  Geological Province: Yilgarn Craton.||||||07-NOV-08
29481|Springhill Member|63454|5|Briefly described|p71 Tb. 2|||Abbreviated version of Springhill Limestone Member.||||||
38812|Springwell Volcanic Complex|23931|6|Mentioned|p202|Archean|Archean|Probably misspelt -s ee Spring Well Complex.||||||07-NOV-08
39290|Stag Sand|24246|6|Mentioned|p18|||Local name for Muderong Shale. Geological Province: Carnarvon Basin||||||24-FEB-05
39290|Stag Sand|66126|6|Mentioned|p215|||Carnarvon Basin. Deposition ceased upon marine transgression marked by Muderong Shale.||||||
80041|Steer Formation, lower|67268|6|Mentioned|p5|||||Mount Barren Group||||
70717|Steptoe Beds''|62453|6|Mentioned|p37|||Informal name.||||||
40113|Steptoe beds""|23571|6|Mentioned|p10|||Informal name - upgraded to Steptoe Formation (Cockbain and Hocking, 1989) Geological Province: Officer Basin.||||||16-MAY-05
40113|Steptoe beds""|24161|6|Mentioned|p13|||Informal - see Steptoe Formation.||||||
83154|Stirling Group|72491|6|Mentioned|p2|||Appears as Stirling Gp.||||||
29021|Stirling Range shale|33445|6|Mentioned|p6|||Age dates||||||
27902|Stirling-Barren Series""|36551|6|Mentioned|p141|||||||||
27902|Stirling-Barren Series""|36872|3|Fully described|p78|||||||||
27902|Stirling-Barren Series""|36876|6|Mentioned|p101|||||||||
34555|Stockton Formation""|22820|5|Briefly described|p13|||Of Lord (1955). Superseded by Stockton Group. Geological province: Collie Basin. Contained the diamictite of the now Shotts Formation and the siltstone of the now Morrhead Formation of the Stockton Group.||||||12-AUG-08
23994|Stockyard Basalt|42533|3|Fully described|p58, p60|||Name reserved.||||||
23994|Stockyard Basalt|44149|5|Briefly described|p35 fig 2-30, p38-39|Archean|Archean|Of Murchison Province||Porlell Subgroup||Overlies Lordy Basalt. Is overlain by Woolgra Formation.|Pillowed tholeiites.|
23994|Stockyard Basalt|64891|5|Briefly described|p37 Fig. 2|Archean|Archean|Of Watkins and Hickman (1990) - superseded by Stockyard Basalt Member. Geological province: Murchison Domain.||||||07-FEB-11
23994|Stockyard Basalt|65268|6|Mentioned|p6 fig 4|||||Porlell Subgroup|||Interlayered high-Mg and tholeiitic basalt.|
23994|Stockyard Basalt|70030|6|Mentioned|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Meekatherra Formation.||||
29024|Strathalbyn Beds|42123|6|Mentioned|Fig.4 P213|||||||||
29024|Strathalbyn Beds|46883|6|Mentioned|Fig.1|||||||||
39224|Strelley Granitoid Complex|23895|5|Briefly described|p884 Fig.1|||Geological Province: Pilbara Craton.||||||07-MAR-05
39224|Strelley Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||180 sq. km.|||||Porphyritic syenogranite, granophyre.|
38538|Strelley Group|23813|5|Briefly described|p101|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38538|Strelley Group|23936|6|Mentioned|p13|||Geological Province: Pilbara Craton.||||||
73870|Strelley Pool Granite|24590|6|Mentioned|p205|||Misspelt? or refers to a granite in the Strelley Pool vicinity?||||||07-FEB-11
73263|Strelley granite|61205|5|Briefly described|p548, p549|||Informal name. Geological Province: Pilbara Craton. Of the Sulphur Springs Group. Overlain by Kangaroo Caves Formation.||||||17-MAY-07
39771|Strelley granitoid|24193|14|Not recorded|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
39772|Strelley pegmatite group|24193|5|Briefly described|p875|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
34391|Strelley succession|22715|5|Briefly described|table7 p214|Archean|Archean|Age: 3270-3200Ma||||||07-NOV-08
34391|Strelley succession|61266|6|Mentioned|p55|||||||||12-MAY-06
83075|Strelly Pool Formation|73160|6|Mentioned|p2 Fig.1|||Pilbara Craton.||Kelly Group||||
23995|Strickland Member|42598|3|Fully described|p99|early Barremian|late Hauterivian|Technically invalid, although reserved.  Strickland Gorge Formation, Tas, has priority.||||||
80107|Stuart Dyke Dolerite|69729|5|Briefly described|p84-85|Neoproterozoic|Neoproterozoic|Mostly NW-trending dykes extending from SE Gawler Craton to the west Musgrave Province.|c.827-824 Ma.|||||
34434|Stuart dyke swarm|22716|6|Mentioned|p238|Stenian|Stenian|Age: 1080 Ma.||||||
34434|Stuart dyke swarm|44114|5|Briefly described|p341|||Arunta Inlier. Sm-Nd age by Zhao and McCulloch (1993). This ~1076 Ma age is significantly older than the ~900 Ma Rb-Sr age of Black et al. (1980). It is very similar to the Alcarra (Kulgera) dyke swarm 500km to the south.|1076 +/- 33 Ma.|||||
40091|Stuart suite|24115|5|Briefly described|p30|Mesoproterozoic|Mesoproterozoic|Age: c. 1070 Ma.||||||
41892|Sue Coal Measures""|12758|6|Mentioned|p9|||Informal - see Sue Coal Measures, now upgraded to Sue Group.||||||
25500|Sue Coal Member|36257|6|Mentioned|Table 2.1|||||||||
38964|Sulphur Spring Group|23807|5|Briefly described|p110|Archean|Archean|Misspelt - see Sulphur Springs Group.||||||07-NOV-08
38964|Sulphur Spring Group|61252|6|Mentioned|p65, p66-67 Fig.2|||||||||
38964|Sulphur Spring Group|73160|6|Mentioned|p12|Paleoarchean|Paleoarchean||3.25-3.24 Ga|||||
69904|Sulphur Springs Group, lower|61256|6|Mentioned|p340 Fig. 5a|Archean|Archean|||||||07-NOV-08
69562|Sulphur Springs volcaniclastics|23891|6|Mentioned|p98|||Informal - see Sulphur Springs Group. Geological Province: Pilbara Craton.||||||
40824|Sunbeam Group, Lower|50188|6|Mentioned|p10 Fig. 3|||Informal - see Sunbeam Group.||||||16-JUL-08
40824|Sunbeam Group, Lower|64283|5|Briefly described|p50 Fig. 1|Neoproterozoic|Neoproterozoic|Informal - see Sunbeam Group. Geological Province: Oldham Inlier.||||||07-FEB-11
40825|Sunbeam Group, Upper|50188|5|Briefly described|p10 Fig. 3|Neoproterozoic|Neoproterozoic|Informal - see Sunbeam Group. Age: ~800Ma.||||||16-JUL-08
40825|Sunbeam Group, Upper|64283|5|Briefly described|p50 Fig. 1|Neoproterozoic|Neoproterozoic|Informal - see Sunbeam Group. Geological province: Oldham Inlier.||||||07-FEB-11
41469|Sunders Creek Formation|50437|6|Mentioned|p5.7|||Intruded by San Sou Suite.||||||
69381|Sundowner basalt|60980|5|Briefly described|p142 Fig.2, p144|||Informal name.||||||27-JUN-05
77539|Sunrise Dam Mine Sequence|66880|6|Mentioned|p16. |Archean|Archean|An informal name for a unit in Kurnalpi Sequence, Kurnalpi Terrane.|2715 +/- 5 Ma.|||||
25503|Surprise Group|29852|6|Mentioned|p409|||||||||
82276|Sweeney Mia Sandstone|69558|6|Mentioned|p95|Early Devonian|Silurian|[?misspelling of Sweeney Mia Formation?] Known from drilling in the area.||||||27-MAY-21
37058|Sweeny Mia Formation|12471|6|Mentioned|p475 Fig.2. |Early Devonian|Early Devonian|||||||27-OCT-14
37058|Sweeny Mia Formation|12729|6|Mentioned|Figs. 3, 22 and 23|||Misspelt. See Sweeney Mia Formation.||||||17-SEP-15
37058|Sweeny Mia Formation|23726|5|Briefly described|p13|||Underlying unit Kopke Sandstone. Geological Province: Carnarvon Basin.||||||
37058|Sweeny Mia Formation|71146|5|Briefly described|p6|Emsian|Emsian|Southern Carnarvon Basin.||||Overlies the Kopke Sandstone.|Halite, evaporite.|
40434|Sweetwater Well Member|24578|5|Briefly described|p786|Paleoproterozoic|Paleoproterozoic|Misspelt - see Sweetwaters Well Member.||||||07-NOV-08
36901|Sweetwaters Dolomite Member|23600|5|Briefly described|p16|||New name for proposed member of the Yelma Formation. Of Yelma Formation. Yerrida Basin.||||||
36901|Sweetwaters Dolomite Member|62289|6|Mentioned|p30 Fig.29|||Misspelling of Sweetwaters Well Member. Of Yelma Formation. Dolomite containing microbial laminations with stromatolite forms.||||||
36901|Sweetwaters Dolomite Member|66427|5|Briefly described|p50 Fig.7 |||Name replaced by Sweetwaters Well Member; see references to that unit at p44 Tb.2, p46 Fig.4, p47, p51, p70-71, p73.|||||Dolomite containing microbial lamination with stromatolite forms; altered to chert at and near the surface.|
81552|Sweetwaters Member|71484|6|Mentioned|p122,130|||Obsolete; member status raised to formation status. See Sweetwaters Well Dolomite.||||||30-AUG-19
32536|Sweetwaters Well Member|23529|5|Briefly described|p10|||Stromatolitic dolomite. Of the Yelma Formation. Geological Province: Earaheedy Basin.||||||26-MAY-09
32536|Sweetwaters Well Member|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation, Earaheedy Basin.||||||07-NOV-08
32536|Sweetwaters Well Member|23589|3|Fully described|p20|Statherian|Statherian|Dolomite and chert breccia at the contact of the Frere Formation. 1700 Ma (Pb isotope (galena)). Of Yelma Formation. Overlain by Frere Formation. Earaheedy Basin.||||||17-JUL-08
32536|Sweetwaters Well Member|24017|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation?||||||07-NOV-08
32536|Sweetwaters Well Member|24578|5|Briefly described|p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation. Geological Province: Earaheedy Basin.||||||26-MAY-09
32536|Sweetwaters Well Member|50188|2|Defined|p3, 5|Paleoproterozoic|Paleoproterozoic|Stromatolitic dolomite facies at the top of the Yelma Formation.  Maximum Thickness: 151m. Type area in text. Overlain by Frere Formation.||||||14-MAR-13
32536|Sweetwaters Well Member|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation. Stromatolite dolomite. Age: <2027Ma. Geological Province: Earaheedy Basin.||||||20-JUN-13
32536|Sweetwaters Well Member|50222|5|Briefly described|p320 Fig. 3, p327|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation (Tooloo Subgroup, Earaheedy Group).  Stromatolitic carbonate facies.  Age: 1.74-1.77Ga (Teen, 1996) and 1.65Ga (Richards and Gee, 1985).  Max. thickness: 100m.  Geological Province: Earaheedy Basin.||||||07-NOV-08
32536|Sweetwaters Well Member|50223|5|Briefly described|p346, p356|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation (Tooloo Subgroup, Earaheedy Group).  Stromatolitic carbonate unit.  Age: ca.2.01 and 1.95Ga (Karhu and Holland, 1996; Russell et al, 1994).  Max. thickness: 100m.||||||07-NOV-08
32536|Sweetwaters Well Member|50226|5|Briefly described|p425|||Of the Yelma Formation.  Includes stromatolitic carbonate rocks; with sulphide and sulphate mineralisation.  Geological Province: Earaheedy Basin.||||||05-DEC-06
32536|Sweetwaters Well Member|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation (Earaheedy Group).  Stromatolitic dolomite, microbial limestone and chert breccia.  Geological Province: Earaheedy Basin.||||||07-NOV-08
32536|Sweetwaters Well Member|61564|5|Briefly described|p591|||Of the Yelma Formation. Chert breccia derived from microbial limestone; minor sandstone. Pervasively silicified.||||||05-DEC-06
32536|Sweetwaters Well Member|62289|6|Mentioned|p29|||In lower part of Yelma Formation. See also misspelled Sweetwaters Dolomite Member.||||||
32536|Sweetwaters Well Member|63866|5|Briefly described|p166|||Eraheedy Basin.||Yelma Formation||||
32536|Sweetwaters Well Member|64284|5|Briefly described|p59|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation (Tooloo Subgroup). Outliers of this member unconformably overlie Terrida Group near twon of Wiluna. Geological Province: Earaheedy Basin. Carbonates formed in a saline lagoonal environment; contains lead-zinc-copper-sulphide deposits.||||||07-FEB-11
32536|Sweetwaters Well Member|64285|5|Briefly described|p66 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Yelma Formation - created as a result of revision of the Earaheedy Group.||||||07-FEB-11
32536|Sweetwaters Well Member|64580|4|Described|map legend||Paleoproterozoic|Of Yelma Formation. Stromatolitic dolomite and limestone; lesser siltstone and sandstone.||||||15-DEC-08
32536|Sweetwaters Well Member|64772|4|Described|p9, Plate 1 legend,  p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of upper Yelma Fm (Earaheedy Gp). Age: <1990Ma. Thickness: ~100m. Geological province: Earaheedy Basin. Stromatolitic and laminated dolomite, locally brecciated and commonly chertified; minor siltstone and sandstone are present; hosts sulfide mineralisation. See also  p25 Fig.11, p28 Fig.16, p33 Fig.21, p35-37, p45 Fig.31, p49-51.||||||25-NOV-13
32536|Sweetwaters Well Member|65472|4|Described|p3 Fig.2, p4, p6, p7 Fig.5, p8 Fig.6|||Thickness: ~100 m. Age: from Fig.2, after Pirajno et al. Deposited carbonates in saline coastal-lagoonal environment. Mississippi Valley-type strata bound mineralisation is present at various localities. Earaheedy Basin. Mentioned as Sweetwaters Member on p1. Also shown on p10, p16, p17 Fig.15a.|2.0-1.94 Ma Pb-Pb carbonate|Yelma Formation||overlain by Frere Formation.|100m thick stromatolitic and algal carbonate facies, with sandy dolomite and dolomitic feldspathic sandstone beds at top and bottom of dolomitic succession; MVT mineralisation; variably altered to chert due to surface weathering.|25-SEP-15
32536|Sweetwaters Well Member|65692|6|Mentioned|p56|||||Yelma Formation.||||
32536|Sweetwaters Well Member|65899|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Yelma Formation, Earaheedy Group. Stromatolitic dolomite and limestone; lesser siltstone and sandstone.||||||
32536|Sweetwaters Well Member|66427|5|Briefly described|p44 Tb.2, p46-47, p51-52, p70-71, p73|||c.100 m thick. Galena mineralisation c.1700 Ma (Pb-Pb; Richards and Gee, 1985). See also reference to former name, Sweetwaters Dolomite Member, on p50 Fig.7.||Unit in Yelma Formation.||Is overlain by Frere Formation.|Stromatolitic dolomite with sandy dolomite and dolomitic feldspathic sandstone beds at top and bottom of the dolomitic succession.|
32536|Sweetwaters Well Member|68055|5|Briefly described|p75, 77-78, 87-88|Proterozoic|Proterozoic|Earaheedy Basin. ~100m thick. Hosts Mississippi Valley-type base-metal mineralisation: carbonate-hosted Zn-Pb sulfides over ~50km strike length. Occurs as chert breccias in surface exposures.||Yelma Formation.|||A stromatolitic dolomite unit.|
32536|Sweetwaters Well Member|69003|5|Briefly described|p14 Fig.18, p15|||Earaheedy Basin. 100m thick.||Yelma Formation.||Is overlain ?conformably by Frere Formation.|Stromatolitic carbonate rock.|
32536|Sweetwaters Well Member|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Yelma Formation|||stromatolitic dolomite and limestone; lesser siltstone and sandstone|
32536|Sweetwaters Well Member|69313|6|Mentioned|p25 Fig.4.3|||||Yelma Formation||||
32536|Sweetwaters Well Member|69596|6|Mentioned|p10|||Earaheedy Basin.||Yelma Formation.||||
32536|Sweetwaters Well Member|70153|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_geologyp14_lut.csv.|1946 +/- 71 - 1811 +/- 13 Ma (isotopic).|Yelma Formation|||Stromatolitic dolomite and limestone; lesser siltstone and sandstone.|
32536|Sweetwaters Well Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, sedimentary breccia|
32536|Sweetwaters Well Member|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Capricorn Orogen. Of Earaheedy Basin. ||Unit of Yelma Formation.|||Stromatolitic and laminated dolomite, locally brecciated and commonly chertified. Minor siltstone and sandstone interbeds are present within the member; some microbial limestone.|
37107|Syenite Camp suite|23751|5|Briefly described|p16|Orosirian|Orosirian|Age: c.1835-1815 Ma. Of Sally Downs supersuite.||||||
37107|Syenite Camp suite|66845|4|Described|p537 Fig.3, p538, p539, p542, p543 Fig.9|||Mount Christine Granitoid (older and younger portions) are assigned to two different parents (Syenite Camp Suite and Kevins Dam suite, respectively) in Tb1. SHRIMP U-Pb zircon dating results.||Sally Downs supersuite|Mount Christine Granitoid (older)||medium- to coarse-grained, even-textured or weakly porphyritic biotite granodiorite and tonalite, with subordinate biotite monzogranite; minor hornblende-bearing granodiorite and monzogranite; mafic enclaves|
37107|Syenite Camp suite|66846|4|Described|p548-p554, p556-p559|Orosirian|Orosirian|Assigned to the Sally Downs supersuite. Transitional chemistry between the Mabel Downs and Kevin Downs suites. Age range probably from U-Pb SHRIMP dating of zircon (see p547). See also: most tables and figures. Rare earth element abundances given on p551 Tb. 2.|1825-1813 Ma|Sally Downs supersuite|||Biotite (-hornblende) granodiorite, tonalite and monzogranite. Even textured to porphyritic.|12-AUG-20
37107|Syenite Camp suite|72437|4|Described|p9, p11, p99-101|Palaeoproterozoic|Palaeoproterozoic|Includes four plutons of granodiorite and monzogranite [which are not named], three of which occur at the southern end of the Lamboo Complex. May also include a phase of the Loadstone Monzogranite and several unnamed sheets and plugs. Twenty seven whole rock analyses are presented.|c. 1835-1805 Ma|Sally Downs supersuite|Includes the Grimpy Monzogranite, Mount Fairbairn Granite, Syenite Camp Granodiorite, Corrara Granite.||Granitoid and coeval gabbro.|
79183|Sylvia Formation|65757|5|Briefly described|p81 Tb.2, p87 Fig.7|||[Misspelling of Mount Sylvia Formation, see p84 Fig.2] overlies Wittenoom Formation, ferruginous siltstone, ferruginous shale, chert||||||
39773|Tabba Tabba pegmatite group|24193|5|Briefly described|p875|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
72784|Table Hill zirconolite|62234|5|Briefly described|p131|||Informal reference to zirconolite within thin sections of Table Hill Volcanics rock.||||||
33953|Table Hills Volcanics|22561|5|Briefly described|p21|||575 +/- 40 Ma.   Officer Basin.||||||
41132|Table Well granite|24196|5|Briefly described|p69|Archean|Archean|Informal name. Age: ca. 2665 Ma (SHRIMP U-Pb zircon: Cassidy et al., 2002) Geological Province: East Agnew-Mount Clifford sub-domain.||||||07-NOV-08
41132|Table Well granite|71310|5|Briefly described|p783 Fig.12|||Agnew-Wiluna greenstone belt.|c.2665 Ma.||||Porphyritic granite.|
75918|Tabletop Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in lower Coonterunah Subgroup. Age shown as >3515 Ma. Amphibolite; metamorphosed mafic volcanic and intrusive rocks; locally schistose.||||||
75918|Tabletop Formation|66217|6|Mentioned|p14. |||East Pilbara Terrane, Pilbara Craton. Not exposed on COONGAN map area.||Unit in Coonterunah Subgroup.||||
83038|Tabletop Intrusives|73184|6|Mentioned|p194|Calymmian|Calymmian|[May be informal name?]|ca 1.59-1.55 Ga|Rudall Complex||||
78540|Tabletop granitic complex|44111|6|Mentioned|p.56, Fig. 1|||in Tabletop Terrane, Rudall Complex?||||||27-NOV-13
80134|Taincrow Granite|69583|6|Mentioned|p43|||Youanmi terrane or Murchison Terrane? A post-kinematic pluton. See also Taincrow Monzogranite (p49, p52).||||||27-SEP-17
25509|Talbot Well Beds|38988|6|Mentioned|p16|||||||||
76075|Talbot Wells Formation|61861|5|Briefly described|pp22-24.|Paleoproterozoic|Paleoproterozoic|Has subdued outcrop. 500 m thick. See also Talbot Well Formation (p3 Table 1).||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
76075|Talbot Wells Formation|70291|4|Described|p180|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami.||Unit of Birridudu Group.|||Silicified carbonate with minor sandstone, siltstone and shale|
83391|Talbot formation|73391|4|Described|vii, 54-55, 57, 59-60, 75, 78-79, 81-82|||See also p85, 113, 118, 132, 174, 188, 194-195, 243-245, 247, 304, 309-311, 314, 316, 319-326, 329, 336-340, 347, 351, 364-365, 417, 420, 422, 441-443, 445, Appendices. New name (this study) proposed for the Black Flag Series: the sedimentary rocks overlying the Upper Basalt. Kalgoorlie district, Eastern Goldfields Province. Lithology described in detail; photographs. Stratigraphic columns; deformation described in great detail. The Golden Mile Dolerite intrudes the unconformable contact with underlying Paringa Basalt.|2696 +/- 2 Ma - 2689 +/- 2 Ma.|||Overlies Centenary Shale, Upper, Gleeson's, Victorious Basalts. Is overlain by (Lower) White Flag Formation (locally unconformably). Correlated with Centenary Shale.|Sandstone, siltstone, intraformational breccia, shale, quartz-rich coarse sandstone, feldspar-rich coarse sandstone, microdiorite porphyry sills and dykes (with local Au-sulphide mineralisation).|
81356|Talbot rhyolites|70095|5|Briefly described|p16,18|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Informal name used to collectively describe rhyolitic units in the Talbot Sub-basin. They reflect dry, ferroan, alkali-calcic to alkali (K-rich) magmas; significant enrichments in F, HFSE, REE, Th and U (Smithies et al., 2013, 2015a). Broadly divided between low-and high-Th/Nb trends, essentially reflecting units associated with the Kaarnka caldera cluster (high Th/Nb) and units with extensive regional stratigraphic continuity (low Th/Nb). Isotopically (more radiogenic Nd and Hf composition) different from Musgrave Province basement.||||||
39760|Talga Talga Sub-group|24194|6|Mentioned|p906 Fig.6|||See also Talga Talga Subgroup||||||
70573|Tamala Limestone Formation|61521|6|Mentioned|p4 Tb.1|||Probably misspelt - see Tamala Limestone.||||||
70573|Tamala Limestone Formation|69840|6|Mentioned|p185|Pleistocene|Pleistocene|Synonymous with Tamala Limestone. Parallel to the coast this unit is  located between Quindalup Dune System (Safety Bay Sand) and Bassendean Dune System (Bassendean Sand).|||||Microbialite.|
29041|Tamala formation|40367|6|Mentioned|Fig.4 p75 (caption)|||Informal - see Tamala Limestone.||||||07-AUG-07
70572|Tamala limestone|40400|6|Mentioned|p114 Fig. 2B|||Informal - see Tamala Limestone.||||||
70572|Tamala limestone|61521|6|Mentioned|p4|||Informal - see Tamala limestone.||||||
70572|Tamala limestone|62732|6|Mentioned|p5|||Informal - see Tamala Limestone.  Averages 60-70% carbonate, containing molluscs and foraminifers as well as minimal quartz and feldspar.||||||05-OCT-06
75180|Tamala limestones|65027|6|Mentioned|p294|||Informal name.||||||16-APR-09
34107|Tambina Granite|22615|4|Described|p 6, 7|||||||||
73584|Tambina Granite""|63441|6|Mentioned|p35|||Term now obsolete. Now interpreted to represent an anticlinal fold in the Shaw Granitic Complex rather than a separate granitic complex or intrusion (Van Kranendonk 2003).||||||07-FEB-11
73585|Tambina Granitic Complex""|63441|6|Mentioned|p35|||Term now obsolete. Now interpreted to represent an anticlinal fold in the Shaw Granitic Complex rather than a separate granitic complex or intrusion (Van Kranendonk 2003).||||||07-FEB-11
37862|Tambina Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
37862|Tambina Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
37862|Tambina Granitoid Complex|24531|5|Briefly described|p25|Archean|Archean|Age: 3450Ma in the core of the complex.  See also p8.||||||07-NOV-08
37862|Tambina Granitoid Complex|24532|5|Briefly described|Map legend|Archean|Archean|Age: >3463Ma.||||||07-NOV-08
80102|Tambina Suite|70826|5|Briefly described|p8|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Intrusion accompanied deposition of the Warrawoona Group.|||||Granites.|12-MAY-20
40530|Tambourah Granite|24531|6|Mentioned|p9|||See also Tambourah Monzogranite.||||||
39774|Tambourah granitoid|24193|14|Not recorded|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
81868|Tanami Supergroup|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen. Also referred to as the Tanami Group on 572. Of Crispe et al, 2007.|||Includes the Dead Bullock Group.|||
34777|Tandalgo Formation|22814|5|Briefly described|fig2|Devonian|Devonian|||||||
26925|Tandalgoo Red beds|22767|5|Briefly described|Table3 p18, p11||Middle Devonian|||||||09-FEB-18
26925|Tandalgoo Red beds|36632|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
26925|Tandalgoo Red beds|43173|6|Mentioned|11||Early Devonian|||||||
27580|Tandalgoo Sandstone|7433|5|Briefly described|p25 Fig.2, p29, p30 Fig.6, p52.|||Canning Basin. Contains an aquifer at considerable depth.||||Overlies Carribuddy Formation. Inferred to partly grade into Poulton Formation.|Fine- to coarse-grained, variably porous red bed sandstone.|
27580|Tandalgoo Sandstone|38878|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early - Middle DevonianE - M||||||
27580|Tandalgoo Sandstone|41169|6|Mentioned|p141|||||||||
27580|Tandalgoo Sandstone|41730|6|Mentioned|Fig.3|||||||||
27580|Tandalgoo Sandstone|42030|4|Described|p746|||||||||
27580|Tandalgoo Sandstone|42338|5|Briefly described|Table 1 P145|||||||||
27580|Tandalgoo Sandstone|42347|6|Mentioned|Fig.2 P1020|||||||||
27580|Tandalgoo Sandstone|42792|5|Briefly described|Table 1 P225|||||||||
27580|Tandalgoo Sandstone|42880|5|Briefly described|Fig.2,p1020|||||||||
27580|Tandalgoo Sandstone|43563|6|Mentioned|p9|||||||||
27580|Tandalgoo Sandstone|43818|6|Mentioned|Fig.2.p39|Middle Devonian|Early Devonian|||||||
27580|Tandalgoo Sandstone|44143|4|Described|p428, p439 Tb.4-19, p442, p443 Fig.4-98|Early Devonian|Early Devonian|Up to 1,000 m thick; red-brown sandstone; aeolian and fluvial. Disconformably overlies Worral Formation. Type section between 1,128 and 1,727m in Sahara 1 (SAHARA: 21deg 04' 40" S, 124deg 23' 30" E). Contains fish scales. Appears as Tandalgoo Formation on p428.||||||24-NOV-17
27580|Tandalgoo Sandstone|45158|3|Fully described|p26|||||||||
27580|Tandalgoo Sandstone|61021|5|Briefly described|p36 Fig. 2|Givetian|Emsian|Geological Province: Canning Basin. See also p39.||||||17-DEC-07
27580|Tandalgoo Sandstone|61551|6|Mentioned|p351 Fig.2. |Givetian|Emsian|||||||
27580|Tandalgoo Sandstone|64643|5|Briefly described|p3 Fig. 2|Middle Devonian|Lower Devonian|||||||
27580|Tandalgoo Sandstone|64982|6|Mentioned|p698.|Early Devonian|Early Devonian|Name replaced by Tandalgoo Formation.||||Unconformably overlies Worral Formation. Is unconformably overlain by Mellinjerie Limestone.||
27580|Tandalgoo Sandstone|69029|6|Mentioned|p319|Givetian|Emsian|Of Canning Basin.||||Overlain by Gogo Formation or Laurel Formation or Grant Group. Underlain by Worral Formation.||
27580|Tandalgoo Sandstone|69297|6|Mentioned|p337, p352|Givetian|Eifelian|Broome Platform of the Canning Basin. ||||Overlain by the Dominic Shale.||
27580|Tandalgoo Sandstone|71870|5|Briefly described|p3|Givetian|Emsian|Canning Basin.||||Unconformably overlies the Sahara Formation.||
69165|Tandalgoo formation|61139|5|Briefly described|p42 Fig. 4|Devonian|Devonian|Geological Province: Canning Basin.||||||
80508|Tangadee rhyolite|63866|5|Briefly described|p162, p168|Statherian|Statherian|Informal sub-unit of the Coobarra Formation?|1638 +/- 14 Ma (SHRIMP U-Pb, Nelson, 1995)|Coobarra Formation||||29-MAR-18
24008|Tanndulla Group|40837|6|Mentioned|Fig.13|||||||||
24008|Tanndulla Group|43818|6|Mentioned|Fig.2.p39|Middle Devonian|Early Devonian|||||||
24008|Tanndulla Group|65449|5|Briefly described|p3, p8-9, p13|||Lehmann (1984), who also included the Worral Formation. In this Report, is regarded as genetically less closely related to this unit than to the Carribuddy Group and is thus included in neither. Appears as Tandulla Group on p3, p9.|||Tandalgoo and Poulton Formations.|||
80369|Tanpool beds|67855|6|Mentioned|p221|||[Historical use only] Of Williams (1968). Incorporated into Mount Minnie Group.||||||07-FEB-18
80296|Tararra Formation|71146|5|Briefly described|p6|Cambrian|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Antrim Plateau Volcanics. Overlain by the Hart Springs Sandstone.|Carbonate and mudstone.|
40115|Tarcunyah Group, Lower|24161|6|Mentioned|p7|||Informal - see Tarcunyah Group.||||||
40115|Tarcunyah Group, Lower|64283|5|Briefly described|p50 Fig. 1|Neoproterozoic|Neoproterozoic|Informal - see Tarcunyah Group. Geological Province: Oldham Inlier.||||||07-FEB-11
69968|Tarcunyah group|50228|6|Mentioned|p482|||Informal - see Tarcunyah Group.||||||
25520|Taurus-Rocky Dam complex|36869|6|Mentioned|p42|||||||||
70189|Teague Granite syenite|61564|6|Mentioned|p590|||Informal reference to syenite within the Teague Granite unit. ||||||
70174|Teizi anorthosites|44109|4|Described|p70|||Consists of anorthosite (nearly 100% plagioclase), orthopyroxene-plagioclase gneiss and rare orthopyroxene rocks. Max. thickness: ~1500m. ||||||
70175|Teizi anorthositic suite|44109|6|Mentioned|p44|||Informal name. See also Teizi anorthosites. Part of the Giles Complex in the Tomkinson Ranges area. ||||||
24021|Telfer Formation|23758|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Renamed Telfer Member of the Malu Formation. Geological Province: Yeneena Basin.||||||
24021|Telfer Formation|23900|4|Described|p1537 Fig. 2|Proterozoic|Proterozoic|Of the Lamil Group. Overlies the Malu Quartzite. Overlain by the Puntapunta Formation. Geological Province: Paterson orogen.||||||
24021|Telfer Formation|24194|5|Briefly described|p900 Fig.3|Neoproterozoic|Neoproterozoic|Sandstone, shale and dolomite. Parent: Lamil Group. Geological Province: Paterson Orogeny||||||
24021|Telfer Formation|36551|6|Mentioned|Table 22|||||||||
24021|Telfer Formation|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24021|Telfer Formation|37212|6|Mentioned|p13|||See also Table 1.||||||
24021|Telfer Formation|37460|4|Described|Table3.VII|||||||||
24021|Telfer Formation|37707|6|Mentioned|Table I|||||||||
24021|Telfer Formation|41066|5|Briefly described|1 of 2 AO2|||||||||
24021|Telfer Formation|42161|6|Mentioned|p49|||||||||
24021|Telfer Formation|42344|5|Briefly described|p54|||1100 Myr||||||
24021|Telfer Formation|43278|4|Described|p644,Fig.2.|Neoproterozoic|Neoproterozoic|Informally subdivided into mine sequence units.||||||
24021|Telfer Formation|43862|5|Briefly described|Fig.2 p378|||||||||
24021|Telfer Formation|43867|5|Briefly described|p199,201|||Hosts gold deposits. Informally subdivided into local mine sequence units.||||||
24021|Telfer Formation|43868|5|Briefly described|p153|||||||||
24021|Telfer Formation|44139|5|Briefly described|p277-281|Neoproterozoic|Neoproterozoic|Chin et al. (1982). 600-700 m. Sandstone, siltstone, shale; minor dolomite, dolomitic shale. Northeastern zone of Yeneena Basin. Includes the auriferous Middle Vale Siltstone Member and Outer Siltstone Member (Turner 1983). Various stratigraphic subdivisions tabulated. Conformably overlies Isdell Formation south of Telfer. Overlies Malu Quartzite. Overlain by Puntapunta Formation. Hosts gold mineralisation.| | ||||06-MAR-18
24021|Telfer Formation|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
24021|Telfer Formation|62453|6|Mentioned|p68|||Superseded by Telfer Formation. ||||||
24021|Telfer Formation|67202|5|Briefly described|p190|||Shown as a unit in the upper Yeneena Group, in a diagram modified after Rowins et al. (1997).|||||Intercalated sandstone and siltstone.|
70464|Ten Mile Rocks|62093|6|Mentioned|p217|Paleoproterozoic|Paleoproterozoic|Appears to be an informal name - described as 'granitic rocks' by Nelson et al (1995) along with Dalyup Gneiss. Age: 1700-1600Ma. Geological Province: at boundary between Biranup Complex and Yilgarn Craton.||||||07-NOV-08
32056|Terrys Camp Member|22905|5|Briefly described|p53-54|Mesoproterozoic|Mesoproterozoic|Marks the base of the Kiangi Creek Formation.  Thick bedded quartz sandstone and siltstone.  Overlies Cheyne Springs Formation.||||||20-MAY-04
32056|Terrys Camp Member|24183|2|Defined|p1, p14|Calymmian|Statherian|Basal unit of the Kiangi Creek Formation. Newly defined unit (Martin, D. McB. & Thorne, A.M. 2002). Age: 1620-1462 Ma.||||||21-MAR-11
32056|Terrys Camp Member|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Kiangi Creek Formation (Edmund Group).  Geological Province: Edmund Basin.||||||07-NOV-08
32056|Terrys Camp Member|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Kiangi Creek Formation (Edmund Group). Geological Province: Edmund Basin.||||||07-NOV-08
32056|Terrys Camp Member|63869|5|Briefly described|p32-33|||Martin et al.,(1999); Martin and Thorne,(2002). Name abandoned because the unit is not regionally distinctive.||Basal unit in Kiangi Creek Formation.|||Dominantly sandstone.|
40778|Teutonic Bore Complex|24196|5|Briefly described|p8|Archean|Archean|Age: 2692 +/- 4 Ma (Nelson, 1995). Geological Province: Yilgarn Craton. Comprises of strongly deformed interbedded andesite, pillow basalt, silicic volcaniclastic rocks and rhyolite lava (Brown et al., 2001)||||||07-NOV-08
40778|Teutonic Bore Complex|24494|5|Briefly described|p14|Archean|Archean|Age: 2692 +/- 4 Ma (U-Pb; Nelson 1995) Andestie and pillow basalt interbedded with thick beds of silicic volcaniclastic rocks and rhyolite lava.||||||07-NOV-08
40778|Teutonic Bore Complex|68109|6|Mentioned|p660|Neoarchean|Neoarchean|Gindalbie Terrane.|c.2690 - 2680 Ma.||||Bimodal rhyolite-basalt and felsic calc-alkaline volcanic complex.|08-OCT-14
40778|Teutonic Bore Complex|71148|6|Mentioned|p121|Neoarchean|Neoarchean|Kurnalpi Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Hosts high-grade Teutonic Bore, Jaguar and Bentley Cu-Zn deposits. Presented as Teutonic Bore Volcanic Complex.|c.2692 Ma.|||||
38655|Teutonic Bore complex|23786|5|Briefly described|p22|||Informal name.  Geological Province: Yilgarn Craton.||||||
38655|Teutonic Bore complex|24196|6|Mentioned|p42|||Informal - see Teutonic Bore Complex||||||
41133|Teutonic Bore volcanic complex|24196|6|Mentioned|p44|||Informal - see Teutonic Bore Complex.||||||
41133|Teutonic Bore volcanic complex|73631|5|Briefly described|p2|Archean|Archean|Hosts the VHMS deposits in the Teutonic Bore Camp.|c.2690 Ma (U-Pb zircon, Nelson, 1995).|||Forms the eastern boundary to the Kent Complex.|Pillow basalt overlain by and interlayered with volcanoclastic units, rhyolite, andesite and thin sedimentary units.|
69025|Teutonic Bore-Melita suite|60976|6|Mentioned|p16|||Informal name. Bimodal calc-alkaline basalt high silica rhyolite.||||||
27910|Thaduna Greywacke|7161|5|Briefly described|p92 Fig.4, p94, p97|||Neds Creek Basin. Channel lobe deposit.||||Laterally equivalent to the Johnson Cairn Shale.|Vertically stacked low-stand-fan turbidites and condensed section mudrocks.|
27910|Thaduna Greywacke|12099|6|Mentioned|p678 Fig.4, p681|||Formerly considered to include the Ravelstone Formation. Equivalent to Thaduna Formation? Placed in Glengarry Group by Gee (1987) and Gee and Grey (1993)||||||
27910|Thaduna Greywacke|22493|5|Briefly described|p94|||||||||
27910|Thaduna Greywacke|22694|6|Mentioned|p7|||now know as Ravelstone Formation||||||
27910|Thaduna Greywacke|23153|6|Mentioned|p83|||||||||
27910|Thaduna Greywacke|23600|6|Mentioned|p8|||Renamed Thaduna Formation.||||||
27910|Thaduna Greywacke|23747|6|Mentioned|p13|||||||||
27910|Thaduna Greywacke|23798|5|Briefly described|p2|||See also Thaduna Formation - names used interchangeably. Of Bryah Group. Thick turbidite sequence of fine-grained, lithic, feldspathic and mafic wacke with subordinate interbedded slaty mudstone. Overlies Narracoota Volcanics. Geol.Prov: Yilgarn Craton.||||||05-JUL-06
27910|Thaduna Greywacke|35975|3|Fully described|p102|||||||||
27910|Thaduna Greywacke|40297|6|Mentioned|p109|||||||||
27910|Thaduna Greywacke|40937|6|Mentioned|p28|||||||||
27910|Thaduna Greywacke|40938|6|Mentioned|p11|||Mention Fig.5||||||
27910|Thaduna Greywacke|40989|4|Described|p16|||See also p21.||||||16-FEB-09
27910|Thaduna Greywacke|42260|6|Mentioned|p125|||||||||
27910|Thaduna Greywacke|43069|5|Briefly described|p18|||of Glengarry Group||||||
27910|Thaduna Greywacke|49893|5|Briefly described|p13|Proterozoic|Proterozoic|Superseded by the Thaduna Formation.||||||
27910|Thaduna Greywacke|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Superseded by Thaduna Formation.||||||
27910|Thaduna Greywacke|61217|5|Briefly described|p45|||Probably misspelt - see Thaduna Formation. Of the Bryah Group. Thick turbidite sequence of fine-grained lithic, feldspathic and mafic wacke with subordinate interbedded slaty mudstone. Overlies the Narracoota Volcanics.||||||07-FEB-11
27910|Thaduna Greywacke|62289|6|Mentioned|p4 Fig. 2, p14|Palaeoproterozoic|Palaeoproterozoic|Gee (1979, 1987), superseded by Thaduna Formation (Occhipinti et al. 1997); outcrops of Thaduna Greywacke in Bryah Basin are now assigned to Ravelstone and Narracoota Formations of Bryah Group (Occhipinti et al. 1997, Pirajno et al. 2000).||||||
27910|Thaduna Greywacke|64384|5|Briefly described|p78 Tb. 8|||Of the Glengarry Group. Geological province: Glengarry Sub-basin. Mafic-derived turbidites, greywacke.||||||07-FEB-11
27910|Thaduna Greywacke|65419|5|Briefly described|p24, p25.|Paleoproterozoic|Paleoproterozoic|Previously Thaduna Beds (of MacLeod, 1970); later Thaduna Greywacke of Gee (1979); revised by Gee (1987) and further revised in this article. Outcrops on western Peak Hill 1:250 000 sheet are now assigned to the Ravelstone and Narracoota Formations. Age from galena veins, reported by J. Richards in Gee (1990); however these veins are in the Ravelstone Formation.|1900 Ma (Pb-Pb isochron).|||||
27910|Thaduna Greywacke|67855|5|Briefly described|p204,  tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. Zero to 5km thick arkose-basalt-greywacke rift facies. Galena from veins in this unit give Pb-Pb model ages of 1.8 Ga (J.R. Richards).||Glengarry Group||||
27910|Thaduna Greywacke|70804|5|Briefly described|p2, p16|||Obsolete name, replaced by the Thaduna Formation of the Mooloogool Subgroup.||||||
68021|Thaduna Metasediments|23798|6|Mentioned|p4 Fig. 2|||Informal reference to rocks of Thaduna Formation. Geological Province: Yilgarn Craton.||||||05-JUL-06
36900|Thaduna beds""|23600|6|Mentioned|p3|||||||||
68020|Thaduna metasediments|23798|6|Mentioned|p3|||Informal reference to rocks of Thaduna Formation. Geological Province: Yilgarn Craton.||||||05-JUL-06
29053|Thambrong Siltstone|32648|6|Mentioned|p32|||in Lyons Gp.||||||
29053|Thambrong Siltstone|37295|6|Mentioned|Table 2|||||||||
30715|The Granites Supersuite|23363|5|Briefly described|356|Orosirian|Orosirian|Age: 1800-1824Ma.||||||21-SEP-06
30715|The Granites Supersuite|50589|5|Briefly described|p1.2, 2.1|Paleoproterozoic|Paleoproterozoic|Age: ~1810Ma. Geological Province: Granites-Tanami Block. See also: Granites Suite, Granites Supersuite.||||||07-NOV-08
30715|The Granites Supersuite|71267|6|Mentioned|1M_geologyp12_lut.csv||||||Includes Slatey Creek Granite.|||
69747|The Wart Gabbro|61340|5|Briefly described|Map legend|||Presented as the compound name The Wart Gabbro/Pyroxenite Intrusion.||||||
69748|The Wart Pyroxenite|61340|5|Briefly described|Map legend|||Presented as the compound name The Wart Gabbro/Pyroxenite Intrusion.||||||21-SEP-05
69754|The Wart gabbro/pyroxenite intrusion|44109|4|Described|p9, p50-55|Mesoproterozoic|Mesoproterozoic|Informal name for part of the Giles Complex mafic-ultramafic intrusions. Also referred to as The Wart intrusion. Forms a sliver of of interlayered gabbro and pyroxenite, overlain by more massive gabbro. Within the Tomkinson Ranges area. ||||||
69754|The Wart gabbro/pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: ~1900m. Possibly a basal segment of Bell Rock Troctolite/Gabbro.||||||21-SEP-05
33225|Thirindine Shale|44657|14|Not recorded|p.12|||Lower Murchison River area.||||||
39763|Thorssell Group|24194|6|Mentioned|p909|||Misspelt - see Throssell Group||||||
39762|Thossell Group|24194|6|Mentioned|p909|||Misspelt - see Throssell Group||||||
70014|Three Corner Bore Conglomerate|61526|5|Briefly described|p879|||Basal conglomerate of banded-iron fragments - occurs where this unit truncates Woongara Rhyolite.||||||
80950|Three Corner Bore Member|71808|5|Briefly described|ix, p42|||Hamersley Province.||Said to be Turee Creek Group.||Correlated with glacial drop-stones in Boolgeeda Iron Formation.|Diamictite, ?glacial.|27-APR-19
81533|Three Corners Bore Conglomerate|71112|5|Briefly described|p79|Rhyacian|Rhyacian|Geological province: Ashburton Province, Pilbara Craton. Of the Horseshoe Basin (intracontinental rift basin).  Also called Three Corners Bore Member on p79 in Fig 12. Preserves bar-and-channel structures typical of gravelly braided-river deposits at Mount Wall.||Unit of Beasley River Quartzite.||||30-AUG-19
80030|Three Corners Conglomerate Member|67130|5|Briefly described|p3 fig 2, p4, p39|||[Misspelling of Three Corner Conglomerate Member]||Beasley River Quartzite|||Coarse conglomerate with abundant clasts of banded iron formation with subordinate mudstone and carbonate.|20-SEP-17
80030|Three Corners Conglomerate Member|68280|5|Briefly described|p5, p44|||||Cheela Springs Basalt||Overlain by Beasley River Quartzite|Conglomerate.|
80030|Three Corners Conglomerate Member|69754|6|Mentioned|p317|||Pilbara Craton.||Beasley River Quartzite||||
80030|Three Corners Conglomerate Member|70086|5|Briefly described|p196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Beasley River Quartzite.||Lowermost unit of the Beasley River Quarzite. Underlain unconformably by Kazput Formation/Turee Creek Group/Mount Bruce Supergroup.||
78629|Three Mile Intrusion|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||||Gabbro; metamorphosed.|07-AUG-15
78629|Three Mile Intrusion|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Gabbro; metamorphosed.|
78629|Three Mile Intrusion|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton.|||||Gabbro; metamorphosed|
31873|Throssell Group|22716|5|Briefly described|table4, p237|Mesoproterozoic|Mesoproterozoic|||||||
31873|Throssell Group|22816|5|Briefly described|p10 Fig. 4|Mesoproterozoic|Mesoproterozoic|Gibson Sub-Basin||||||
31873|Throssell Group|22907|6|Mentioned|40 fig 1|||||||||
31873|Throssell Group|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Yeneena Supergroup, Yeneena Basin.||||||
31873|Throssell Group|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yeneena Supergroup.||||||
31873|Throssell Group|23583|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province Yeneena Basin.||||||
31873|Throssell Group|23585|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of Yeneena Supergroup. Overlying unit Lamil Group. Underlying unit  Rudall Complex. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23590|2|Defined|p9, p22 Appendix 2|Neoproterozoic|Mesoproterozoic|Age: <1300 to c.1100 Ma (poor age constraints). Of Yeneena Supergroup. Overlying unit Lamil Group. Underlying unit Rudall Complex. Geological Province: Yeneena Basin. Max. thickness: 5500 m.||||||
31873|Throssell Group|23594|4|Described|p21|Neoproterozoic|Mesoproterozoic|Age: 900-1300 Ma. Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23602|5|Briefly described|p7|Proterozoic|Proterozoic|Age: 1250-900 Ma. Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23730|4|Described|p9|Neoproterozoic|Mesoproterozoic|Age: c.1300-850 Ma. Of Yeneena Supergroup. Underlying unit Rudall Group. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23742|4|Described|p6||Mesoproterozoic|Of Yeneena Supergroup. Overlying unit Tarcunyah Group.||||||
31873|Throssell Group|23745|4|Described|p16|Neoproterozoic|Mesoproterozoic|Age: 1300-900 Ma. See also page 7 Fig 5. Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23746|4|Described|p24|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup.||||||
31873|Throssell Group|23758|5|Briefly described|p2 Fig 1|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23760|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
31873|Throssell Group|23780|5|Briefly described|p189|Mesoproterozoic|Mesoproterozoic|||||||
31873|Throssell Group|23900|4|Described|p1537 Fig. 2|Proterozoic|Proterozoic|Of the Yeneena Supergroup. Overlain by the Lamil Group. Geological Province: Paterson orogen.||||||
31873|Throssell Group|24025|4|Described|p15|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup.  Geological Province: Pilbara Craton.||||||
31873|Throssell Group|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Parent: Yeneena Supergroup. Geological Province: Yeneena Basin||||||
31873|Throssell Group|24194|4|Described|p897|Neoproterozoic|Mesoproterozoic|Parent: Yeneena Supergroup. Overlying Unit: Lamil Group. Geological Province: Yeneena Basin||||||
31873|Throssell Group|24197|5|Briefly described|p100|||Formerly of the Yeneena Group. Includes the Broadhurst Formation. Geol. Prov: Paterson Orogen.||||||07-FEB-11
31873|Throssell Group|24594|5|Briefly described|p602|Neoproterozoic|Mesoproterozoic|Age: ca1070-680Ma.  Unconformably overlies Ruddall Complex.  Geological Province: Yeneena Basin (Paterson Orogen).See also p601.||||||
31873|Throssell Group|43848|5|Briefly described|Map Legend||Proterozoic|of Yeneena Supergroup.||||||
31873|Throssell Group|43849|5|Briefly described|Map Legend||Proterozoic|Of Yeneena Supergroup. [invalid name - Throssell Shale in Kimberleys has priority]||||||
31873|Throssell Group|44111|6|Mentioned|p.55, 56 Fig.1, 57, 60|||Supersedes part of Yeneena Group. Deposited between 1790 and 1290 Ma. Underwent three episodes of deformation and greenschist facies metamorphism between 1290 and 820 Ma. Unconformably underlies Tarcunyah Group. Contains significant mineralisation, including base metals and uranium; also minor PGE and REE.||||||
31873|Throssell Group|44189|5|Briefly described|Map legend||Proterozoic|||||||
31873|Throssell Group|44190|5|Briefly described|Map Legend||Proterozoic|||||||
31873|Throssell Group|44831|5|Briefly described|Map Legend||Proterozoic|||||||
31873|Throssell Group|44866|5|Briefly described|Map Legend||Neoproterozoic|||||||
31873|Throssell Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
31873|Throssell Group|49895|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Of the Yeneena Supergroup. Geological Province: Paterson Orogen. Overlain by the Tarcunyah Group. see also p2 Fig.1.||||||
31873|Throssell Group|49911|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Sandstone, fine- to medium-grained and well-bedded; minor interbedded siltstone and shale.  Age: >900Ma.  Geological Province: Yeneena Basin.||||||
31873|Throssell Group|50008|5|Briefly described|p45 Fig.2|Neoproterozoic|Neoproterozoic|Geological Province: Yeneena Basin.||||||
31873|Throssell Group|50188|6|Mentioned|p10 Fig. 3|||||||||
31873|Throssell Group|50436|5|Briefly described|p1.1|||Of the Yeneena Group. Includes: Broadhurst Formation.||||||
31873|Throssell Group|50544|5|Briefly described|p56, p10 Fig. 5|Neoproterozoic|Mesoproterozoic|Of the Yeneena Supergroup.  Consists of the basal Coolbro Sandstone, and Broadhurst Formation above.  Age: c.1250-900Ma (Hickman and Bagas, 1999).  Geological Province: Yeneena Basin.  See also p16 Tb. 1, p59-60.||||||
31873|Throssell Group|50555|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Yeneena Supergroup.  Geological Province: Yeneena Basin.||||||21-JUL-04
31873|Throssell Group|60470|6|Mentioned|p1, 2|Neoproterozoic|Neoproterozoic|Informal name replaced by Throssell Range Group. In Yeneena Basin, of Yeneena Supergroup. ||||||
31873|Throssell Group|62453|6|Mentioned|p67|||Superseded by Throssell Range Group. ||||||
31873|Throssell Group|64283|5|Briefly described|p50 Fig. 1, p54 Fig. 4|Neoproterozoic|Mesoproterozoic|Succession of metamorphosed to greenschist facies consisting of a basal sandy interval (Coolbro Sst) overlain by carbonaceous shale, siltstone, turbidite and carbonate units (Broadhurst Fm).||||||07-FEB-11
31873|Throssell Group|64286|6|Mentioned|p74|Neoproterozoic|Mesoproterozoic|Age: ?c.1.0Ga.||||||07-FEB-11
31873|Throssell Group|64772|5|Briefly described|p14 Fig. 7, p35|||Telfer gold mineralisation and metalliferous occurrences are associated with this unit.||||||07-FEB-11
31873|Throssell Group|64943|4|Described|p2-7,13,14,17,19,21,23-24,26,29-33,35,39|Neoproterozoic|Mesoproterozoic|Includes Coolbro Sandstone. Sandstone-shale-carbonate succession; 1250-900 Ma; unconformably overlies Rudall Complex; fault or unconformity with Lamil Group. Metamorphosed to greenschist facies during Miles orogeny. Max age 1333 Ma; min 900 Ma.||||||
31873|Throssell Group|65403|4|Described|p1, pp13-29.|Neoproterozoic|Mesoproterozoic|Deposition interpreted as starting in a rift basin between Pilbara Craton and the ?North Australia Craton. Recumbent folds produced by Miles Orogeny (c.1132 - 800 Ma). Epigenetic galena mineralisation 940-820 Ma.||Unit in Yeneena Supergroup.|Includes Coolbro Sandstone, Taliwanya, Pungkuli and Broadhurst Formations.|Unconformably overlies Rudall Complex. Is overlain unconformably by Karara Formation and is faulted against Tarcunyah Group.||
31873|Throssell Group|65826|6|Mentioned|p5, p11.|||Informal name; superseded by Throssell Range Group.||||||23-MAY-16
31873|Throssell Group|68981|6|Mentioned|p3 Fig.2|||Paterson Orogen.||||||
31873|Throssell Group|69185|5|Briefly described|500k_interpgeop_pilcrat02_lut.csv|Neoproterozoic|Mesoproterozoic|Of Yeneena Basin.|<1070 Ma|Unit of Yeneena Supergroup.||||
31873|Throssell Group|70154|6|Mentioned|2_5m_geologyp98_lut.csv|Mesoproterozoic|Mesoproterozoic|||||||
31873|Throssell Group|70826|6|Mentioned|p11|Neoproterozoic|Neoproterozoic|Rudall Province. Same age as the Centralian Superbasin. Misspelt as Throssel Group.||||||20-MAY-20
31873|Throssell Group|71795|6|Mentioned|p34 fig 3|||Paterson Orogen.||||||
69969|Throssell group|50228|5|Briefly described|p477, p482|Neoproterozoic|Neoproterozoic|Informal - see Throssell Group. Unconformably overlies the Rudall Complex. May be a correlative of the c. 690-605Ma Supersequence 2 of the Centralian Basin?||||||
70718|Throssell'' Group|62453|6|Mentioned|p67|||Informal name. ||||||
34204|Thrussell Shale|22649|6|Mentioned|p 141|||Rb- Sr age 670+/-84 Ma p141.  Kimberly Region||||||
24031|Thundelarra Group|23955|4|Described|p1240, p1242 Fig.3|||Overlain by the Minjar Group. Overlies the Gossan Hill Group. Maximum Thickness: 2800m. Geological Province: Murchison province, Yilgarn Craton.||||||12-JAN-15
24031|Thundelarra Group|41434|6|Mentioned|Fig.2|||||||||
24031|Thundelarra Group|61912|5|Briefly described|p158|||Includes banded iron formation and basalt.||||||
24031|Thundelarra Group|70020|5|Briefly described|p131|||Geological province: Yilgarn Craton. Thickness: 2300-2800m.||Unit of Murchison Supergroup.||Overlain by Minjar Group. Underlain by Gossan Hill Group.||
24031|Thundelarra Group|70270|6|Mentioned|p519, p519 Fig. 2, p520 Fig. 3|||||Of Murchison Supergroup.||||29-JUN-18
24031|Thundelarra Group|71168|6|Mentioned|p11, p12 fig 6, p13 fig 7|||Yilgarn Craton.||||Overlies Gossan Hill Group, underlies Minjar Group.||
79601|Thundellara Supersuite|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2950 Ma.||Bunnawarra Suite, Gnows Nest Granodiorite.|||
29258|Tickalara metamorphics|31230|6|Mentioned|p182|||Map legend||||||
68873|Tickalara psammopelite|60533|6|Mentioned|p594, p595 Fig. 4|||Informal reference to a part of the Tickalara Metamoprhics.||||||05-MAY-05
68874|Tickalara psammopelites|60533|6|Mentioned|p594|||Informal reference to a part of the Tickalara Metamorphics.||||||
31131|Ticklara Metamorphics|23568|5|Briefly described|p2775|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen.||||||07-NOV-08
31131|Ticklara Metamorphics|23621|6|Mentioned|p19|||||||||
31131|Ticklara Metamorphics|23714|5|Briefly described|p8|||Geological Province: Halls Creek Mobile Zone.||||||
31131|Ticklara Metamorphics|43484|6|Mentioned|10|||||||||
31131|Ticklara Metamorphics|43561|6|Mentioned|p1436|||Formed before approx 1865 Ma||||||
31131|Ticklara Metamorphics|43586|5|Briefly described|p3,Fig.1,p4|||||||||
31131|Ticklara Metamorphics|43595|6|Mentioned|p350|||||||||
31131|Ticklara Metamorphics|43632|6|Mentioned|p2|||Included within Biscay Formation||||||
31131|Ticklara Metamorphics|43794|5|Briefly described|p319||Proterozoic|||||||
31131|Ticklara Metamorphics|44230|5|Briefly described|Map Legend||Proterozoic|||||||
81748|Tikalara Metamorphics|67323|5|Briefly described|p29|||A turbidite package deposited in an oceanic island arc setting between the Kimberley Craton and the North Australian Craton.|~1865-1860 Ma.|||||
36910|Tjingkulatjatjarra Formation""|23602|6|Mentioned|p9|||||||||
82054|Toby gabbro|72437|5|Briefly described|p59|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Biotite gabbronorite.|
77784|Toby intrusion|60498|5|Briefly described|p1016 Fig.1, p1017, pp1019-1020, p1022.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name, except for the caption referring to 'mafic-ultramafic intrusions'. Halls Creek Orogen. A high-level evolved mafic intrusion forming dipping sheets and faulted blocks. Little economic potential. Electron microprobe geochemical analyses of apatites and biotites are detailed.|1855 +/- 2 Ma (Page & Hoatson 2000).||||Layered mafic-ultramafic intrusion: subophitic biotite gabbro, olivine gabbro, gabbro, dunite.|03-JAN-18
77784|Toby intrusion|63866|5|Briefly described|p133, p138|||Western Zone, Halls Creek Orogen.|c. 1855 Ma (inferred emplacement)||||Biotite-quartz gabbro, biotite gabbro, olivine gabbro and minor troctolite.|
77784|Toby intrusion|69003|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. A single high-level mafic intrusion.|1855 +/- 2 Ma.|||||
78870|Tollu Granite|67128|5|Briefly described|p12|||Also appears as Tollu granite (p25).|1073 +/- 6 Ma (Kirkland et al., 2009).||||Massive, medium- to fine-grained, porphyritic granite; tabular, euhedral, perthite phenocrysts up to 2cm. Rare rapakivi texture; biotite clots up to 10% of the rock.|
78870|Tollu Granite|69153|6|Mentioned|GA_geochron.csv|||Sample 90984015 from Tollu Granite, west of Mummawarrawarra, Western Musgrave Block. Sun, S.S. Gray, C.M. Sheraton, J.W. 1995. Zircon U-Pb chronology and neodymium isotope study of tectono-thermal and crustal forming events in the Tomkinson Ranges, western Musgrave Block, Central Australia|||||Felsic intrusive, MT-BT granite|
79627|Tollu granite|68996|5|Briefly described|p7, 39, 43, 50, 51, 52,56,57,62,64,65|Mesoproterozoic|Mesoproterozoic|[Informal,invalid name. Tollu Group has precedence] Characterized by low density and low susceptibility. Its geometry is a shallowly north-dipping disc that reaches a maximum thickness of ~5 km. Shown as Tollu granitoid p67.|1076+/-9 Ma U/Pb SHRIMP|Giles Suite, Warakurna Supersuite||||
77420|Tollu group|65907|6|Mentioned|p6.|||[Mis-print (?) of Tollu Group]||||||01-MAY-15
70437|Toodyay Stone|61273|5|Briefly described|p85|Archean|Archean|Dimension stone quarried as quartzite flagstones in the Perth region. Colour varies from milky  white to grey, or from cream to red-brown; commonly exhibits thin. pale-green bands of fuchsite along cleavage planes.||||||07-NOV-08
39186|Toolina Limestone facies""|23768|5|Briefly described|p31|Late Eocene|Late Eocene|Informal name - see Toolina Limestone.||||||30-MAR-05
37218|Toolina limestone|23989|5|Briefly described|p54 Fig. 46|Late Eocene|Late Eocene|Informal name. Geological Province: Yilgarn Craton||||||03-MAR-10
78749|Toologa Calcilutite|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|[Mis-spelling of Toolonga].||||||
40297|Toolonga Calcilutite""|23915|6|Mentioned|p539|Cretaceous|Cretaceous|Informal-see Toolonga Calcilutite.||||||
77469|Toolonga Formation|12491|6|Mentioned|p454 Fig.7.|||Presented in figure as Korojon, Withnell, Toolonga Formations. Carbonates.||||||06-NOV-14
77469|Toolonga Formation|68811|5|Briefly described|p46 fig 21, p160 tbl 23 |Cretaceous|Cretaceous|[Misspelling of the Toolonga Calcilutite].|||||Calcilutite mud.|16-APR-20
75178|Toolonga limestone and chalk|65027|5|Briefly described|p294|Late Cretaceous|Late Cretaceous|Informal name. Forms basement rocks in the area.||||||
41209|Tooloo Subgroup, lower|50222|6|Mentioned|p337|||Informal - see Tooloo Subgroup.||||||
70459|Tooloonga Calcilutite|60709|5|Briefly described|p859|Campanian|Coniacian|Probably misspelt - see Toolonga Calcilutite. Geological Province: Perth Basin||||||
26179|Top Camp Formation|24183|5|Briefly described|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin. Of the Bangemall Group.||||||
26179|Top Camp Formation|40089|2|Defined|p39|Mesoproterozoic|Mesoproterozoic|||||||
26179|Top Camp Formation|44142|4|Described|p309 Fig.4-13, p310 Tb.4-3, p314 Tb.4-4|||See also p317. Originally Top Camp Dolomite (Halligan and Daniels, 1964); contained four named Members (Muhling and Brakel, 1985); following work by Chuck (1984), now correlated with units in Edmund Subgroup; here recommended this unit become obsolete (Williams, 1990). 900-2500m thick. Unit in proposed subdivision of Bangemall Group by Muhling and Brakel (1985).||Edmund Subgroup.||Overlain by Fords Creek Shale conformably.|Dolomite, limestone, shale, dolomitic shale, chert, quartz arenite, breccia; minor conglomerate.|
74046|Torrens Member|13242|5|Briefly described|p214 Fig. 2, p215|Late Permian|Late Permian|Name stated to be informal by author. This is a possible lower member of the Pearce Formation in the Hyland Bay Sub-group.||||||07-FEB-11
80214|Tower Hill Monzogranite|71166|5|Briefly described|p73, p75 fig 3.58|Neoarchean|Neoarchean|[unclear if this is a formal name or an informal mine site name]. Leonora Camp.|2750 Ma|||||05-OCT-17
80214|Tower Hill Monzogranite|73596|6|Mentioned|p1164|Neoarchean|Neoarchean|Kalgoorlie-Kurnalpi Rift. Presented informally as Tower Hill biotite monzogranite.|2753 +/- 6 Ma (Fletcher et al., 2001).|||||
41134|Tower Hill granite|24196|6|Mentioned|p69 Fig.10|||Geological Province: East Agnew-Mount Clifford sub-domain.||||||
26182|Towers Formation|22615|6|Mentioned|p 3|||||||||
26182|Towers Formation|23206|6|Mentioned|p1260|||of Warrawoona Group||||||
26182|Towers Formation|23755|6|Mentioned|p6|||Of Warrawoona Group||||||
26182|Towers Formation|23783|5|Briefly described|p14|||Of Salgash Group.||||||01-APR-16
26182|Towers Formation|23807|5|Briefly described|p127|||Geological Province: Pilbara Craton.||||||
26182|Towers 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
26182|Towers Formation|24184|4|Described|p699|Archean|Archean|Overlying Unit: Apex Basalt. Geological Province: Pilbara Craton. Now divided into 3 distinct units (Van Kranendonk, 2000):- Dresser Formation, Marble Bar Chert Member and Strelley Pool Chert.||||||07-NOV-08
26182|Towers Formation|24185|5|Briefly described|p743 Tb.4|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
26182|Towers Formation|24194|5|Briefly described|p905|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
26182|Towers Formation|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
26182|Towers Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Salgash Subgroup (Warrawoona Group). Blue, black, white layered chert. Age: <3463Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
26182|Towers Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Basal unit of Salgash Subgp. Three red/white/grey banded chert members separated by (pillow) basalt, komatiite, felsic volcanics or sediments; middle member is Marble Bar Chert Mbr. Overlain by Apex Basalt. Age: 3433+/-2Ma. Max. thick: 500m. See also p130||||||07-FEB-11
26182|Towers Formation|31309|2|Defined|p53|Archean|Archean|||||||07-NOV-08
26182|Towers Formation|38498|5|Briefly described|Table 1|||See also Fig.1.||||||
26182|Towers Formation|38544|6|Mentioned|Fig.1|||||||||
26182|Towers Formation|39672|6|Mentioned|Fig.2|||||||||
26182|Towers Formation|39697|3|Fully described|p93|||||||||
26182|Towers Formation|40596|6|Mentioned|Fig.1|||||||||
26182|Towers Formation|41028|6|Mentioned|p227|||||||||
26182|Towers Formation|41624|6|Mentioned|p43|||||||||
26182|Towers Formation|41767|6|Mentioned|p45|||||||||
26182|Towers Formation|41938|6|Mentioned|Fig.1 P10|||||||||
26182|Towers Formation|43057|6|Mentioned|Fig.2.9|||||||||
26182|Towers Formation|43595|6|Mentioned|Fig.2-47,211|||||||||
26182|Towers Formation|43698|6|Mentioned|p26|||||||||
26182|Towers Formation|43769|6|Mentioned|Fig.3,p858|||||||||
26182|Towers Formation|44150|4|Described|p129 Tb.2-15, p132 Figs.2-131,-132|||See also p133 Tb.2-16, p152 Tb.2-22, p157 Fig.2-144. 500m thick. Formerly Hong Kong Chert (of Fitton et al., 1975) and part of Sharks Formation (Ingram, 1977). Main stratigraphic marker within Warrawoona Group; traceable for 430 km. Either precipitate or diagenetic silicification; preserved stromatolites and filamentous colonial microfossils are oldest-known well-preserved fossils on Earth.|c.3.5 Ga.|Salgash Subgroup|Includes Marble Bar Chert Member.||Up to three chert members separated by basalt, komatiite, felsic volcanics or sediments.|
26182|Towers Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group (Pilbara Supergroup). Geological Province: Pilbara Craton.||||||07-NOV-08
26182|Towers Formation|50544|5|Briefly described|p22|||On MARBLE BAR sheet; absent on the YARRIE sheet.  Separates Duffer Formation and Apex Basalt.||||||
26182|Towers Formation|60429|5|Briefly described|p9|||Absent on MUCCAN - but separates the Apex Basalt above from the Duffer Formation below in MARBLE BAR area.||||||07-FEB-11
26182|Towers Formation|60636|5|Briefly described|p52|||Of Warrawoona Gp. Separates Duffer Fm from overlying Apex Basalt in the Marble Bar Greenstone Belt. It consists of the thin discontinuous Chinaman Pool Chert, a basalt unit and the Marble Bar Chert. See also p35-36 Fig. 3.2.||||||07-FEB-11
26182|Towers Formation|61111|6|Mentioned|p108|||Actually discussed in relation to cherts from Towers and Apex Basalt Formations.||||||
26182|Towers Formation|61266|4|Described|p58 Tb.1|Archean|Archean|Of the Salgash Group (Warrawoona Group). Age: <3463 Ma. Blue-black and white layered chert, barite. Geological Province: Pilbara Craton.||||||01-APR-16
26182|Towers Formation|62427|5|Briefly described|p3 Fig.2, p4, p6, p7 Fig.4, p13  |||Marble Bar Greenstone Belt.||Of the Warrawoona Group||Overlies Duffer Formation.|Sandstone, chert, silicified basalt and minor felsic volcanic rock.|
26182|Towers Formation|63441|5|Briefly described|p6 Tb. 1, p19-20|Archean|Archean|Name abandoned - redefined as Duffer Fm (Warrawoona Gp). Alternating chert units with volcanic rocks now interpreted to be due to local stratigraphic intercalation. Its former chert units, Chinaman Pool and Marble Bar Chert Members now part of Duffer Fm.||||||07-FEB-11
26182|Towers Formation|64328|5|Briefly described|p54, p56 Tb. 1|||Subsequently recognised to be Strelley Pool Chert. Chert, basalt.||||||07-FEB-11
26182|Towers Formation|64405|5|Briefly described|p6, p15, p16|||Name given to one of the thicker cherts of Warrawoona Group - subsequently interpreted as Strelley Pool Formation. Summary of previous investigations/interpretations/ subsequent correlations is provided (p6). Also referred to as "Towers Formation".||||||01-APR-16
26182|Towers Formation|64628|5|Briefly described|p170, p184.|Early Archean|Early Archean|Pilbara Craton. Seawater-rock interactions incorporated K in the rocks and liberated Mg into the ocean (Nakamuro and Kato, 2004).||Unit in Warrawoona Group.|||Carbonatized dolerites and pillow basalts.|
26182|Towers Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Warrawoona Group. Includes Marble Bar Chert Member. ||||||
26182|Towers Formation|65008|6|Mentioned|p8 |||||||||
26182|Towers Formation|66217|6|Mentioned|p22, p60.|||Hickman (1977) included in this unit layered red, white and black cherts of the Marble Bar Chert Member, which have been re-assigned by Van Kranendonk et al. (2006a) to the Duffer Formation.||||||
26182|Towers Formation|67668|6|Mentioned|p. 157.|||No longer used in Pilbara stratigraphy. Used in report by Schopf and Packer 1987 on putative cellular microfossils. May be related to/replaced by the  Strelley Pool Formation and/or Euro Basalt.||||||
26182|Towers Formation|70733|6|Mentioned|p106|||Subsequently named Marble Bar Chert Member.||||||
70720|Townsend Formation''|62453|6|Mentioned|p14|||Superseded by Townsend Quartzite.||||||12-DEC-06
70722|Townsend Range Series''|62453|6|Mentioned|p14|||Superseded by Townsend Quartzite.||||||12-DEC-06
70721|Townsend quartzite''|62453|6|Mentioned|p14|||Superseded by Townsend Quartzite.||||||12-DEC-06
77449|Treachery Sequence|67354|6|Mentioned|p100.|||A presumed alternative informal name for Treachery Formation.||||||
41379|Trealla carbonates|60119|6|Mentioned|p25|||Informal - see Trealla Limestone.||||||
78400|Trillbar Member|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Bryah Basin.|c.2000 Ma|Of the Narracoota Formation.|||Interleaved foliated metagabbro, metamicrogabbro, metabasalt, metapyroxenite, and serpentinized metaperidotite; local magmatic layering well preserved.|06-MAY-14
41239|Trillbar complex|50226|6|Mentioned|p422|||Of Myers (1990).  Informal name for unit which is now considered part of the Narracoota Formation (Occhipinti and Myers, 1999).||||||09-DEC-04
81036|Trillbar formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bryah Basin.||Bryah Group, lower|||Gabbro, microgabbro, mafic and ultramafic schist; minor mafic rock; metamorphosed.|
24043|Tripod Hill Formation|22534|6|Mentioned|Fig.5 p10|||of Kalgoorlie Group||||||
24043|Tripod Hill Formation|41066|6|Mentioned|2 of 2 I03|||||||||
24043|Tripod Hill Formation|41588|4|Described|p244|||||||||
24043|Tripod Hill Formation|41784|6|Mentioned|Table 1|||||||||
24043|Tripod Hill Formation|62108|6|Mentioned|p1409 Tb. 1|||Another name for Kambalda Komatiite.||||||07-FEB-11
40289|Tripod Hill Member, upper|24322|5|Briefly described|p58|Archean|Archean|Informal.  Of the Kambalda Komatiite Formation.  Of the Kambalda Group.||||||07-NOV-08
29078|Triumph Dolerite|22596|6|Mentioned|Table 1 p409|Archean|Archean|||||||07-NOV-08
29078|Triumph Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
29078|Triumph Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
41089|Triumph gabbro|24139|5|Briefly described|p239 Table 1|||Geological Province: Kambalda Domain.  Of the Black Flag Beds.||||||
31947|Triwhite sandstone|43876|14|Not recorded|p573|Kungurian|Artinskian|||||||
24045|Troy Creek Beds|22896|6|Mentioned|103|||||||||
24045|Troy Creek Beds|23253|5|Briefly described|p2|||See unnumbered figure. Geological Province:  Earaheedy Basin.||||||12-SEP-05
24045|Troy Creek Beds|23529|6|Mentioned|p7|||Troy Creek Schist of Hocking & Jones (1999).||||||
24045|Troy Creek Beds|24017|6|Mentioned|p7|||Replaced by Troy Creek Schist.||||||
24045|Troy Creek Beds|37460|6|Mentioned|p138|||||||||
24045|Troy Creek Beds|38515|4|Described|p8|||||||||
24045|Troy Creek Beds|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24045|Troy Creek Beds|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24045|Troy Creek Beds|40355|4|Described|p4|||||||||
24045|Troy Creek Beds|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24045|Troy Creek Beds|42708|5|Briefly described|Plate 1|Proterozoic||||||||
40826|Troy Creek Beds""|50188|6|Mentioned|p3|||Of Bunting et al (1982) and Commander et al (1982) and amended but not defined by Hocking and Jones (1999). Superseded by Troy Creek Schist and then abandoned when recognised as metamorphosed Earaheedy Group rocks. Geol.Prov: Earaheedy Basin.||||||16-JUL-08
40826|Troy Creek Beds""|64772|5|Briefly described|p9|||Of Bunting et al (1982); Commander et al (1982). Now obsolete. Originally thought to be an older suite of metamorph'd rocks unconformable below Yelma Fm - now considered to be  metamorph'd sed. rocks of Earaheedy Group, deformed in the Stanley Fold Belt.||||||07-FEB-11
34952|Troy Creek Schist|22896|6|Mentioned|103|||Previously Troy Creek Beds||||||
34952|Troy Creek Schist|23529|6|Mentioned|p7|||||||||
34952|Troy Creek Schist|24017|5|Briefly described|p5 Tb. 1|||Name abandoned and rocks incorporated into Earaheedy Group as deformed Yelma, Frere or Chiall Formations.  See also "Troy Creek Schist", p11.||||||
34952|Troy Creek Schist|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
34952|Troy Creek Schist|50188|5|Briefly described|p3, p8|||Formerly Troy Creek Beds of Bunting et al (1982) and Commander et al (1982). Both names now abandoned when recognised as metamorphosed sedimentary rocks of Earaheedy Group. Geological Province: Earaheedy Basin.||||||16-JUL-08
34952|Troy Creek Schist|71484|5|Briefly described|p130|||Geological province: Of Earaheedy Basin. Also referred to as Troy Creek beds on p130. Interpreted to have metamorphosed Yelma Formation.||||||30-AUG-19
38401|Troy Creek Schist""|24017|5|Briefly described|p13|||Informal name.  See also Troy Creek Schist.||||||
81553|Troy Creek beds''|71484|5|Briefly described|p130|||Of Commander et al., 1992. Geological province:  Earaheedy Basin. Metamorphosed to greenschist facies; outcrops along central-northern edge of the basin. Previously interpreted to have an interfingering relationship with Imbin Porphyry.|||||Interbedded phyllite and shale.|30-AUG-19
41135|Trump tonalite|24196|5|Briefly described|p69|Archean|Archean|Informal name. Age: 2670 +/- 10 Ma (SHRIMP U-Pb zircon: Black et al ., 2002) Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||07-NOV-08
40480|Tuckfield Member conglomerates|24466|6|Mentioned|p372|||Informal - see Tuckfield Member||||||
40479|Tuckfield conglomerates|24466|6|Mentioned|p372|||Informal - see Tuckfield Member||||||
29962|Tumbiana Basalt|43055|6|Mentioned|Table 2|||||||||
38091|Tumbiana Formation""|23570|6|Mentioned|p239 Appendix 1|||See Tumbiana Formation.||||||
78751|Tumbiana Sequence|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean|Of Blake (1993). Equivalent to Tumbiana Formation.||Mount Jope Supersequence.||||24-APR-20
32600|Tumbinna Pisolite|23570|4|Described|p239 Appendix 1|||Thought to be the original spelling of Tumbiana Pisolite. Now superseded by Tumbiana Formation.||||||
32600|Tumbinna Pisolite|44152|5|Briefly described|p171-172|||Of Noldart and Wyatt (1962). [Author asserts this is the correct spelling for the place name: Tumbinna Pool, on the Nullagine River; inexplicably mis-spelt as Tumbiana Pisolite by de la Hunty (1963, 1964) and others since.]|||||A sequence of dolomitic rocks with classic oolitic and pisolitic textures.|
32600|Tumbinna Pisolite|45923|3|Fully described|p.67, p80|||Map F51-5, U.Prot?. Named after Tumbinna Pool. Several reference sections described. Reference has been altered by hand on p80 to subsequent spelling of unit : Tumbiana.||||Appears to be interbedded in part with lower beds of the Carawine Dolomite.||23-OCT-15
32601|Tumbinna beds|45923|6|Mentioned|p80|||Variation on Tumbinna Pisolite.||||||
77842|Tumblagooda Group|1943|2|Defined|p376-382, p373, p375 Fig.3, p376 Fig 4|Early Ordovician|Late Cambrian|Formerly Tumblagooda Sandstone. Type section is composite sections near Kalbarri. Clastic dominated. Max. thickness known: 1267m, Kalbarri-1. Age: older than Middle Silurian, probably late Cambrian to earliest Early Ordovician based on fragmentary conodonts.|||Divided into four unnamed Units, based on sequence boundaries. Unit 1 at base; Unit 4 at top.|Is overlain by Dirk Hartog Group. Log correlations from Kalbarri-1 to Yaringa-1 suggest unconformable boundary, although this is not obvious in all wells.||
75618|Tumblagooda Sandstone""|65313|5|Briefly described|p579, Fig.7|Cambrian|Cambrian|Informal subdivision of ?Cambrian part of Tumblagooda Sandstone because: offshore seismic suggests angular unconformity within basal part of unit; Cambro-Ordovician conodonts reported in Wandagee 1 core; and support from pedostratigraphic age model.||||||
35980|Tunney Shale|23379|5|Briefly described|p160 Fig.2||Valanginian|Different from Tunney Member. Invalid name (Tunney Member has priority). of Barrow Sub-basin, Carnarvon Basin.||||||
81576|Turkey Creek intrusion|71873|6|Mentioned|p427,441|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. See Turkey Creek Gabbro.||||||
33842|Turkey Creek microgabbro-norite|22469|6|Mentioned|p18, fig 21||Paleoproterozoic|Halls Creek Province||||||07-NOV-08
33842|Turkey Creek microgabbro-norite|23897|5|Briefly described|p377 Fig.1|||Informal name.||||||
33842|Turkey Creek microgabbro-norite|60498|6|Mentioned|p1016 Fig.1.|Paleoproterozoic|Paleoproterozoic||||||Layered mafic-ultramafic intrusion:|
24541|Turkey Hill Beds|36096|6|Mentioned|Fig.3|||||||||
24541|Turkey Hill Beds|40888|6|Mentioned|p153|||||||||
24541|Turkey Hill Beds|41405|5|Briefly described|p205|||||||||
24541|Turkey Hill Beds|45149|3|Fully described|p27|||See also Table 1.||||||
24541|Turkey Hill Beds|46975|6|Mentioned|p83|||||||||
24541|Turkey Hill Beds|49792|5|Briefly described|Fig.5|||||||||
24541|Turkey Hill Beds|64970|6|Mentioned|p721 Fig. 5|||Informal, should be beds.||||||
70723|Turkey Hill Beds''|62453|6|Mentioned|p47|||Informal Name.||||||
28163|Turkey Hill beds|23282|6|Mentioned|p54|||of western Officer Basin. Synonymous with Chambers Bluff Tillite. of Townson (1985).||||||
28163|Turkey Hill beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|[Superseded by Turkey Hill Formation. CEBMar95]||||||11-MAY-06
28163|Turkey Hill beds|43756|6|Mentioned|p541|||||||||
72435|Twin Hills banded granitic gneiss|73596|6|Mentioned|p1170|Mesoarchean|Mesoarchean|Kalgoorlie-Kurnalpi Rift. Appears shortened to Twin Hills granitic gneiss.|2803 +/- 3 Ma.|||||
79628|Umutju granite|68996|6|Mentioned|p4|||Shows E-W trending fabric.||||||
41136|Union Jack granite|24196|5|Briefly described|p69|Archean|Archean|Informal name. Age: ca. 2665 Ma (SHRIMP U-Pb zircon: Cassidy et al., 2002). Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||07-NOV-08
41136|Union Jack granite|73596|6|Mentioned|p1160|||Kalgoorlie Terrane. Presented as Union Jack monzogranite.||||Intrudes Ballard Gneiss.||
42198|Upper Basalt|50421|4|Described|p285, 286 Fig.2||Archean|Overlies unassigned komatiite. High Mg to tholeiitic. Kalgoorlie Terrane.||||||07-NOV-08
42198|Upper Basalt|64633|6|Mentioned|p21.||||<2692 +/- 4 Ma.|||||
42198|Upper Basalt|73391|4|Described|vii, 15, 17, 19-21, 25, 39, 48, 50-52|||See also p57, 59, 67, 75, 82, 85, 88, 100, 105, 109, 111-114, 116, 132, 147, 172, 174, 188, 194-195, 197, 201-202, 206, 238, 243-244, 252-254, 268, 275, 278-281, 284-286, 289, 293, 296, 304, 306, 310, 315, 317-318, 324-325, 331-333, 347-348, 361-362, 419, 435, 441-442, Appendices. Swager et al. (1990). Kalgoorlie Terrane, Eastern Goldfields Province. Absent in the Coolgardie Domain. Is intruded by a sill dated 2687 +/- 5 Ma. Appears as Upper Basalt Group on p39, and is occasionally referred to as the Upper Basalt Unit (or unit) and Upper Basalt Formation. Hosts magmatic Ni-Cu-PGE.|2687 Ma.||Bent Tree Basalt, Victorious Basalt, Paringa Basalt. ?Golden Mile Dolerite, Williamstown Dolerite.|Overlies Highway Ultramafic. Is overlain unconformably by Spargoville Formation, (Talbot formation), Black Flag Series.|High-Mg komatiitic to tholeiitic mafic volcanic rocks, and co-magmatic mafic-ultramafic sills.|
31385|Upper Birdrong Sandstone|43564|6|Mentioned|p462|||Informal variation on Birdrong Sandstone||||||
33927|Upper Capricorn Megasequence|22512|6|Mentioned|Fig1 P284|||||||||
31425|Upper Carbonate Member|43599|6|Mentioned|p248|||Worral Formation||||||
32328|Upper Cardabia Group|44159|5|Briefly described|Table p.37|Early Eocene|Paleocene|||||||
83077|Upper Chert Member|73160|6|Mentioned|p3-4, p5 Fig.3|||Referred to as Unit II by Terabayashi et al. (2003).||Dresser Formation||||
35982|Upper Dupuy Formation|23379|5|Briefly described|p160 Fig.2;p162|Berriasian|Kimmeridgian|Informal name for that part of the Dupuy Formation above the Dupuy Massive Sands. of Barrow Sub-basin, Carnarvon basin.||||||
29091|Upper Greenstone group|30295|4|Described|p80|||||||||
32772|Upper Holmwood Shale""|45016|14|Not recorded|p.55|||May be equivalent to Carrandibby Formation.||||||
32734|Upper Jarlemai Siltstone|44998|14|Not recorded|App.5 p289|||||||||
32743|Upper Liveringa beds|44998|14|Not recorded|App.4 p282-5|||Contains Hardman fauna.||||||
35056|Upper M. australis Sandstone|22702|4|Described|p104,112||Barremian|Invalid name, should be given a proper name. More often refered to in the same text as upper M. australis Sandstone.||||||09-AUG-05
32885|Upper Madeline Formation|48848|14|Not recorded|p.65|||||||||
77187|Upper Malu Formation|44139|6|Mentioned|p281, Table 3-15|||Informal name (of Turner 1983 PhD thesis).| | ||||10-SEP-12
34111|Upper Mannum Formation|22626|6|Mentioned|446 fig 10|Early Miocene|Early Miocene|Geol province Murray Basin. Overlying unit Finnis Clay, underlying unit Lower Mannum Formation||||||
34109|Upper Morgan Cadell Marl|22626|6|Mentioned|446 fig 10|Middle Miocene|Middle Miocene|Geol province Murray Basin. Underlying unit Lower Morgan Limestone||||||
25571|Upper Muderong Shale|42598|5|Briefly described|Fig.5 after P14|||Variation on Muderong Shale. Probably intended informally.||||||
25571|Upper Muderong Shale|44938|4|Described|p151,Fig.3,152|Aptian|Berriasian|Invalid form of name.||||||
77189|Upper Vale Shale|44139|6|Mentioned|p281, Table 3-15|||Probably informal name of Blockley (1974) after unpublished work of Newmont P/L. Subsequently included in Telfer Formation.| | ||||10-SEP-12
32791|Upper unit|44230|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
32791|Upper unit|44231|5|Briefly described|Map Legend||Proterozoic|Of Pentecost Sandstone.||||||
33227|Uppermost Noonkanbah Formation|44657|14|Not recorded|p.10||Early Permian|(Fitzroy basin). Lower Permian.||||||
77574|Van Emmerick Conglomerate, Upper|66127|5|Briefly described|Plate 1.|Famennian|Famennian|Mapped separately from Van Emmerick Conglomerate and dated as probably Famennian.||||||
77747|Velkerri Formation, Middle|64975|6|Mentioned|p161.|||See Velkerri Formation; there is no formal Middle member.||||||
32580|Venture Slate|23926|5|Briefly described|p9|Archean|Archean|Misspelt - see Agnes Venture Slate.  Of Woolyeenyer Formation.  Geological Province: Yilgarn Crato.||||||07-NOV-08
32580|Venture Slate|45543|4|Described|p.102,105||Archean|Unit of Woolyeenyer Group.||||||07-NOV-08
38579|Victorious basalt|23782|5|Briefly described|p8 Fig. 6|||Geological Province: Yilgarn Craton.||||||
38579|Victorious basalt|23926|6|Mentioned|p10 Tb. 1|||Informal.||||||
38579|Victorious basalt|24139|5|Briefly described|p239 Table 1|||Geological Province: Ora Banda Domain.  Of the Grants Patch Group.||||||
77736|Victorius Basalt|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Ora Banda Domain. Kambalda Sequence. Mis-spelling of Victorious.|||||Tholeiitic and high MgO basalt.|
41470|Violet Valley Granodiorite|50437|6|Mentioned|p4.2|||Geological Province: Kimberley Region. Of the Kevins Dam Suite. Used interchangeably with Violet Valley Tonalite.||||||10-AUG-04
26976|Virgin Hills formation|24000|6|Mentioned|p348|||Informal - see Virgin Hills Formation.||||||
26976|Virgin Hills formation|31870|6|Mentioned|p11|||||||||
26976|Virgin Hills formation|36225|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian to Famennian||||||
26976|Virgin Hills formation|43876|14|Not recorded|p561|Famennian|Frasnian|||||||
80242|Vivien Dolerite|70326|5|Briefly described|p342,350|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. [Is this the same as Vivien Formation? Or Vivien Metasediments? But also listed as alternate name to Turret Dolerite; p350; see also reference cited; Barnes et al., 2014]. Major and trace element geochemical analysis on Table 4 p342-346.||||||
80242|Vivien Dolerite|71308|5|Briefly described|p715|||Agnew-Lawlers area. Of the authors' High-Th Siliceous Basalts group.|||||Basalt with distinctly layered shallow sills, with pyroxene-rich lower cumulate layers and leucogabbro upper layers.|
80242|Vivien Dolerite|72049|6|Mentioned|p253|||This unit has magmatic affinities with the Williamstown Dolerite.||||||
80242|Vivien Dolerite|73238|6|Mentioned|p13 Fig.10|||Agnew district, Mount White Basin, Eastern Goldfields Terrane. Appears in Fig.10 as Vivien (Turret) Dolerite.||||||
80129|Vivien Gabbro|71212|5|Briefly described|intro p2, p46, p55, p89|||Yilgarn Craton. Equivalent to the formal Turret Dolerite. Hosts the Vivien reef gold deposit. See also p133, p146, p228.||||Overlies the White Hope Basalt.||
81580|Vivien Group|72057|5|Briefly described|p238|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||||Equivalent to Black Flag Group.||
79817|Vivien Metasediments|69586|5|Briefly described|p1|||Said to have been renamed the Worrunga Formation.||||||
79817|Vivien Metasediments|71212|4|Described|intro p2, p1, p46, p55, p143|||Yilgarn Craton. Equivalent to the formal Vivien Formation. Potential lateral equivalent of the Scotty Creek Metasediments. Deformation and structural characteristics discussed. Closely associated with large, long-lived crustal scale structures that host significant gold deposits. See also p69, p70, p90, p133, p134, p136, p147, p228, p239-p242, p247, p248, p252, p258, p262, App.D.||||Overlain (structurally) by the Maria Volcanosedimentary Package. Disconformably overlain by the Scotty Creek Metasediments.|Interlayered quartzofeldspathic, clastic to volcaniclastic, possibly tuffaceous sandstones and siltstones with less common dark shales and rare conglomerates and mafic-ultramafic sediments.|
83719|Vivien Sedimentary Formation|70275|5|Briefly described|p471|||Central Mt. Keith portion of the Agnew-Wiluna Belt, Kalgoorlie Terrane, Yilgarn Craton.|2692 +/- 3 Ma.|||Overlies Monument Ultramafic Unit. Is overlain by Mount White Formation.||
83719|Vivien Sedimentary Formation|70276|6|Mentioned|p783, p784 Fig.2|||Agnew-Wiluna greenstone belt, Yilgarn Craton. Appears as Vivien metasedimentary Formation on p783.|2692 +/- 3 Ma.|||||
77541|Vivien Sequence|66880|5|Briefly described|p13, p26. |Archean|Archean|In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank. Agnew Domain, Kalgoorlie Terrane. Identical age to Kapai Slate. Correlative with Kambalda Sequence.|2692 +/- 3 Ma.|||Is overlain by Maria Sequence.|Includes volcanogenic metasandstone.|01-NOV-12
77541|Vivien Sequence|73151|6|Mentioned|p2, p15|||Of Duuring et al., 2010. Equivalent to the Mount White Group?. Has intrusive contacts with regionally extensive granitoid plutonism between 2700 Ma and 2665 Ma in the Eastern Goldfields Superterrane.||||||
42364|Vulcan Formation, Lower|5952|5|Briefly described|p217|||Informal name.||||||05-MAY-09
42364|Vulcan Formation, Lower|7142|6|Mentioned|p350 Fig.4.|Late Jurassic|Middle Jurassic|Browse Basin.||||Overlies Plover and Montara Formations. Is overlain by Upper Vulcan Formation.||
42364|Vulcan Formation, Lower|13292|5|Briefly described|pp308-311.|Late Jurassic|Late Jurassic|See Vulcan Formation. A relatively uniform shale, it is generally regarded as the main hydrocarbon source rock in the Vulcan Graben. Considerable variation in thickness lessens reliability of maturity maps.||||||
42364|Vulcan Formation, Lower|13353|6|Mentioned|p398.|Late Jurassic|Late Jurassic|Use Vulcan Formation. Includes hydrocarbon source rocks.||Unit in Swan Group.||Overlies Plover Formation.||24-JAN-17
42364|Vulcan Formation, Lower|13354|6|Mentioned|p375 Fig.6.|Late Jurassic|Middle Jurassic|Unit of Swan Group. Overlies Plover Formation of the Troughton Group, and underlies Upper Vulcan Formation.||107||||28-OCT-14
42364|Vulcan Formation, Lower|22663|5|Briefly described|AC97 1-4 Fig.4||Late Jurassic|Swan Group||||||
42364|Vulcan Formation, Lower|23378|4|Described|p180 Fig.2; p177-8, 196, 198-201|Kimmeridgian|Oxfordian|Invalid name, part of Vulcan Formation used in the same paper. Should have lower case "l". of Vulcan Sub-basin.||||||
42364|Vulcan Formation, Lower|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Informal name - see Vulcan Formation. Geological Province : Vulcan Sub-Basin||||||
42364|Vulcan Formation, Lower|24207|4|Described|p209-210|Kimmeridgian|Callovian|Geological Province: Vulcan Sub-basin.||||||
42364|Vulcan Formation, Lower|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin. Informal name||||||09-MAR-05
42364|Vulcan Formation, Lower|42053|4|Described|p40|||||||||
42364|Vulcan Formation, Lower|42066|6|Mentioned|Fig.3 p199|||||||||
42364|Vulcan Formation, Lower|42081|5|Briefly described|Fig.2 p291|||||||||
42364|Vulcan Formation, Lower|60378|4|Described|p95, 98, 104-119|Late Jurassic|Late Jurassic|Organic-rich marine succession. Petroleum source rock? Thickness variations and distribution discussed.||presumably informal subdivision of Vulcan Formation||||
42364|Vulcan Formation, Lower|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Late Jurassic|Late Jurassic|The Vulcan Formation is not formally divided into Lower and Upper units.||The Vulcan Formation (without the 'Lower') is a unit in the Swan Group.||||
42364|Vulcan Formation, Lower|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Middle Jurassic|Age: ~156-145 Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||09-NOV-06
42364|Vulcan Formation, Lower|63358|5|Briefly described|p4 Fig. 1.3|Kimmeridgian|Callovian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
42364|Vulcan Formation, Lower|64689|5|Briefly described|p7-14, p17, p19|Tithonian|Oxfordian|Valanginian. Vulcan Sub-basin. Sealing blanket from syn-rift deposition. Source for oil shows in Crux-1 from adjacent Heywood Graben.||||Unconformably overlies Plover Formation. Is overlain by Upper Vulcan Formation.|Syn-rift shale.|
42364|Vulcan Formation, Lower|64696|6|Mentioned|p125, p126, p127 Fig.2, p131|Kimmeridgian|Callovian|See also p134-138, p140. Syn-rift succession. Has important source (basal 20-30 m) and reservoir rocks.||||Overlies Plover Formation unconformably.||
42364|Vulcan Formation, Lower|64697|6|Mentioned|p84 Fig.2, p86, p88, p91-92|Late Jurassic|Late Jurassic|||||||
42364|Vulcan Formation, Lower|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Kimmeridgian|Kimmeridgian|Swan Group. Underlies the Upper Vulcan Formation, overlies the Montana Formation. Mount Ashmore Dome. Shallow marine sandstone and claystone.||||||
42364|Vulcan Formation, Lower|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Is overlain by Upper Vulcan Formation.||
42364|Vulcan Formation, Lower|70061|5|Briefly described|Regional geology Fig.7, p9. Vulcan:Fig.2|Tithonian|Callovian|Contains mature marine, oil- and gas-prone source rocks for all the produced oils in the Vulcan Sub-basin.||Swan Group.|||Predominantly marine mudstones that contain variable amounts of terrigenous organic matter.|12-JUL-16
42364|Vulcan Formation, Lower|70064|5|Briefly described|Regional Fig. 6; p6-8. Central: Fig.2|Tithonian|Callovian|See also Northern: Fig.2; p2. Yampi: Fig.2. Browse Basin. An oil source in the Heywood Graben. Potential reservoir. Forms seals for Plover Formation reservoirs.||Swan Group.||Overlies Troughton Group. Is overlain by Upper Vulcan Formation.||12-JUL-16
42364|Vulcan Formation, Lower|70934|6|Mentioned|unpaginated|Late Jurassic|Late Jurassic|Source rocks in the Swan Graben.|||Elm Sandstone|||
42365|Vulcan Formation, Upper|7142|6|Mentioned|p350 Fig.4.|Early Cretaceous|Late Jurassic|Browse Basin.||||Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||
42365|Vulcan Formation, Upper|12466|5|Briefly described|p173.|Late Jurassic|Late Jurassic|[See Vulcan Formation]. Westralian 2 (W2) oils source rock; hydrocarbons generated from mixed terrestrial and marine organic matter in a clastic marine setting.||||||
42365|Vulcan Formation, Upper|13292|6|Mentioned|pp310-311.|Late Jurassic|Late Jurassic|See Vulcan Formation.||||||
42365|Vulcan Formation, Upper|13353|6|Mentioned|p398.|Early Cretaceous|Early Cretaceous|Use Vulcan Formation. Includes hydrocarbon source rocks.||Unit in Swan Group.||Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||
42365|Vulcan Formation, Upper|13354|6|Mentioned|p375 Fig.6, p383.|Late Jurassic|Late Jurassic|Unit of Swan Group. Overlies Lower Vulcan Formation and underlies Echuca Shoals Formation of the Bathurst Island Group. A suggested source of hydrocarbons in Gwydion 1 well, Yampi Shelf.||187||||28-OCT-14
42365|Vulcan Formation, Upper|22663|5|Briefly described|AC97 1-4 Fig.4|Early Cretaceous|Late Jurassic|Swan Group||||||
42365|Vulcan Formation, Upper|23378|4|Described|p180 Fig.2; p196|Early Cretaceous|Late Jurassic|Invalid name, part of Vulcan Formation used in the same paper. Should have lower case "u". of Vulcan Sub-basin.||||||
42365|Vulcan Formation, Upper|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Informal name - see Vulcan Formation. Geological Province : Vulcan Sub-Basin||||||
42365|Vulcan Formation, Upper|24207|4|Described|p211, p209 Fig. 5|Valanginian|Tithonian|Characterised by thick restricted marine mudrocks and coarse clastic sub-marine fan deposits near inter-graben highs.  Geological Province: Vulcan Sub-basin.||||||
42365|Vulcan Formation, Upper|24427|5|Briefly described|p49 Fig.2|Early Cretaceous|Tithonian|Geological Province: Bonaparte Basin. Informal name.||||||09-MAR-05
42365|Vulcan Formation, Upper|42053|4|Described|p40|||See also Fig.3||||||
42365|Vulcan Formation, Upper|42066|6|Mentioned|Fig.3 p199|||||||||
42365|Vulcan Formation, Upper|60378|5|Briefly described|p95, Fig 2|Early Cretaceous|Late Jurassic|Sometimes a petroleum seal.||presumably informal subdivision of Vulcan Formation||||
42365|Vulcan Formation, Upper|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Early Cretaceous|Late Jurassic|The Vulcan Formation is not formally divided into Lower and Upper units.||The Vulcan Formation (without the 'Upper') is a unit in the Swan Group.||||
42365|Vulcan Formation, Upper|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Age: 145-~137Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||
42365|Vulcan Formation, Upper|63358|5|Briefly described|p4 Fig. 1.3|Valanginian|Tithonian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
42365|Vulcan Formation, Upper|64689|5|Briefly described|p7 Fig.6, p11 Fig.11, p13-15, p17-19|Valanginian|Tithonian|Valanginian. Vulcan Sub-basin. Sealing blanket from syn-rift deposition.|||||Syn-rift shale.|
42365|Vulcan Formation, Upper|64696|6|Mentioned|p127 Fig.2, p134, p135-136|Berriasian|Tithonian|A gas column in this unit, in Kalyptea-1, was sourced from the Echuca Shoals Formation.||||||
42365|Vulcan Formation, Upper|64697|6|Mentioned|p84 Fig.2, p92|Early Cretaceous|Late Jurassic|An oil pool was intersected by Cultus Petroleum's Tenacious-1 in 1997.||||||
42365|Vulcan Formation, Upper|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Berriasian|Berriasian|Swan Group. Underlies the Echuca Shoals Formation, overlies the Lower Vulcan Formation. Mount Ashmore Dome. Deep marine sandstone.||||||
42365|Vulcan Formation, Upper|69689|6|Mentioned|p16|Cretaceous|Jurassic|Browse, Bonaparte Basins.||||Overlies Lower Vulcan Formation. Is overlain by Heywood Formation.||
42365|Vulcan Formation, Upper|70061|6|Mentioned|Regional geology Fig.7. Vulcan: Fig.2|Valanginian|Tithonian|||Swan Group.||||12-JUL-16
42365|Vulcan Formation, Upper|70064|5|Briefly described|Regional Fig. 6; p6, p8. Central: Fig.2|Valanginian|Tithonian|See also Northern: Fig.2; p2. Yampi: Fig.2. Browse Basin.||Swan Group.|Brewster Member.|Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||12-JUL-16
40083|WGF Formation|24207|4|Described|p218|||Not a formal name - compound term for Woolaston, Gibson and Fenelon Formations.  Calcareous claystone, marl and calcilutite composition.  Max. thickness: 300m.  Geological Province: Vulcan Sub-basin.||||||01-MAR-10
75279|Wadarrah Quartz Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Hornblende-bearing quartz monzonite with local platy mineral alignment.||||||07-FEB-11
69378|Wadarrah quartz monzonite|60981|5|Briefly described|p176|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
39250|Wadera Calcarenite Member|24094|5|Briefly described|p275|||Name used interchangably with Wadera Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
25581|Wadera Calcarenite""|41271|6|Mentioned|p166|||||||||
77451|Wadeye Sub-Group|67354|5|Briefly described|p73, p106.|Sakmarian||Of Gorter et al.(2005). The author opines it should probably be included within the Kulshill Group. Siliciclastics. Major sea-level fall and canyon incision at its base from the Namurian to middle Moscovian.||Unit in Weaber Group.|Includes the onshore Point Spring Formation, and the offshore Arco and Aquitaine Formations.|Overlies the Sunbird Formation. Is overlain by Kuriyippi Formation.||
24066|Wadgingarra Basalt|42533|3|Fully described|p65|||Name reserved, but Wadgingarra Gabbro (and Wadingarra Gabbro) already recorded.||||||
24066|Wadgingarra Basalt|44149|5|Briefly described|p35 fig 2-30, p38-40|Archean|Archean|Of Murchison Province||Yalgoo Subgroup||Overlain by Camberathunun Formation.|Bimodal sequence of massive high-Mg and tholeiitic basalt.|
24066|Wadgingarra Basalt|65268|6|Mentioned|p6 fig 4||||||||Tholeiitic basalt.|
79818|Wadgingarra Igneous Complex|69583|6|Mentioned|p49|Mesoarchean|Mesoarchean|Murchison Domain.||||||
79818|Wadgingarra Igneous Complex|69584|6|Mentioned|p5 Fig.2|Neoarchean|Neoarchean|||Meeline Suite||||
79818|Wadgingarra Igneous Complex|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Meeline Suite.||||
32792|Wagina Formation|5257|6|Mentioned|p153|Late Permian|Permian|Perth Basin. Includes Beekeeper Member.||||||
32792|Wagina Formation|23356|5|Briefly described|26 Tab.2|Late Permian|Late Permian|||||||
32792|Wagina Formation|23520|6|Mentioned|p25. p26|||Basal section of thin transgressive sand (Broad and Bradley, 1975) at the unclear Triassic-Permian boundary, is here considered to be the upper part of the Beekeeper Formation.||||||
32792|Wagina Formation|44237|14|Not recorded|p.202||Tatarian|Fig.2.||||||
32792|Wagina Formation|60377|4|Described|p61 Fig. 3, p63|Capitanian|Wordian|Overlain by Dongara Sandstone. Geological Province: Perth Basin. Depositional Environment is shoreface. Consists of sandy shales and siltstones that can be up to 5% Total Organic Carbon (TOC)||||||07-FEB-11
32792|Wagina Formation|60386|5|Briefly described|p297, 304, 313|Guadalupian|Guadalupian|Northern Perth Basin. Fluvial sands. Age shown as ~Late Permian. Includes volcanics dated at 261-267 +/-5 Ma.||||Overlies Carynginia Formation. Coeval with Beekeeper Formation.||
32792|Wagina Formation|61546|5|Briefly described|p381, p382, p385 Fig.5, p386. |Late Permian|Late Permian|Perth Basin. Part of the commercially viable Cliff Head oil field. Transgressive estuarine and marine sediments.||||Is overlain by Dongara Sandstone.||
32792|Wagina Formation|64099|5|Briefly described|p366, p367 Fig. 2|Wuchiapingian|Wordian|Mentioned throughout text as Dongara Sandstone/Wagina Formation. Massive shallow-marine sandstones, minor pebble bands and siltstone. Underlies Kockatea Shale unconformably/conformably. Coeval and interfingering Beekeeper Limestone. Age: Upper Permian.||||||
32792|Wagina Formation|70097|6|Mentioned|p2, p9, p20 Fig.4|||Crostella, 1995; Mory and Iasky, 1996. Now referred to as the Wagina Sandstone. See Wagina Sandstone in this paper. Shown once as Wagina Formation (Dongara Sandstone Member) in North Perth Summary column (Fig.4). [possible accidental use of former names?] Elsewhere in paper, Wagina Sandstone (including in the same column as Wagina Formation in Fig.4) and Dongara Sandstone are used.||||||12-SEP-17
32792|Wagina Formation|71623|5|Briefly described|p349,351, p345 fig 2|Capitanian|Wordian|Perth Basin. Part of Cape Hay Clastic Cycle. Mostly non-marine.|||||Sandstone|
32792|Wagina Formation|73484|6|Mentioned|p476 Fig.3|Lopingian|Guadalupian|Perth Basin. Fluvio-lacustrine.||||||
80028|Wagina Sequence|69297|6|Mentioned|p207|||Play type previously variously referred to as Dongara, Wagina or Wittecarra sequences. Sealed by Kockatea Sequence.||||||20-SEP-17
70696|Wahlgu Formation''|62453|6|Mentioned|p42|||Informal name.||||||
70697|Wahlgu Group|62453|4|Described|p5 Fig. 3, 12 Fig. 8, 22|Ediacaran|Cryogenian|Geological Province: Officer Basin. Underlies: Lungkarta Formation. Overlies: Steptoe Formation.||||||
81314|Waladah gabbro|70020|5|Briefly described|p118|Neoarchean|Neoarchean|Geological province: Yilgarn Craton.||Unit of Yalgowra Suite.||||
77455|Walcott Formation, Lower|67368|6|Mentioned|p209 Fig.4.|Middle Eocene|Middle Eocene|||||||
77456|Walcott Formation, Upper|67368|6|Mentioned|p209 Fig.4.|Early Oligocene|Late Eocene|||||Is overlain by Mandu Formation.||
25584|Walgidee Hill Lamproite|41158|6|Mentioned|Table 54|||Misspelling of Walgidee Hills||||||
76871|Walgunya Trondjhemite|65726|5|Briefly described|Map legend|Archean|Archean|[Mis-spelling of Trondhjemite] East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||Of Mount Edgar Granitoid Complex.|||Quartz-rich biotite trondhjemite, medium- to coarse-grained.|
42405|Wallabi Group|23816|6|Mentioned|p257 Fig.23|||Geological Province: Perth Basin.||||||
41137|Wallaby Knob monzogranite|24196|5|Briefly described|p40|Archean|Archean|Age: 2653 +/- 3 Ma (Black et al., 2002)||||||07-NOV-08
77542|Wallaby Sequence|66880|5|Briefly described|p28, p30.|Archean|Archean|See also Wallaby Conglomerate. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank. Intrusions dated at c.2664 and c.2658 Ma are probably not actual magmatic ages.|2650 +/- 6 Ma (Salier et al. 2004).|||Intruded by syenitic rocks.||01-NOV-12
77567|Wallaby Supersequence|66937|6|Mentioned|p155. |Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin.|||Includes Wallaby Conglomerate and Potoroo Sandstone.|||
77567|Wallaby Supersequence|66938|6|Mentioned|p192. |Archean|Archean|In lower part, amalgamated depositional sequences are aggradationally up to progradationally stacked, implying uplift and sediment flux were outpacing tectonic escape.||||||
38659|Wallaby conglomerate|23786|5|Briefly described|p27|||Informal name - see Wallaby Conglomerate.  Geological Province: Yilgarn Craton.||||||
38659|Wallaby conglomerate|62083|5|Briefly described|p1014 Fig.6, p1015 Fig.7|||Main gold camp: Laverton.|>2664 Ma||||Conglomerate-arenite.|
38659|Wallaby conglomerate|67198|6|Mentioned|p49-51|||See also Wallaby Conglomerate (p49, p55).||||||
38659|Wallaby conglomerate|70292|5|Briefly described|p338, p346 Tb.2, p348, p359|Neoarchean|Neoarchean|Minimum age of 2662+/-3 Ma constrained by titanite U-Pb age of skarn.|2673+/-5 Ma detrital zircon maximum age||||Clast-supported, poorly sorted, and pebble to boulder size. Rare graded beds.|
72615|Wallaby syenite|67198|6|Mentioned|p51, p56|||Syenite dykes and calcite veins have been folded by ductile shearing which is overprinted by brittle deformation that marks first major phase of gold lode development.|||||Syenite dykes, steep dipping calcite veins (with pyrite, biotite and some gold)|08-SEP-17
72615|Wallaby syenite|70292|6|Mentioned|p358|||Considered to be cogenetic with calc-alkaline dikes at Wallaby. Wallaby monzonite-syenite suite also used p358, Wallaby intrusive suite p356.|||||Characterised by phenocrysts of orthoclase.|
41138|Walling Rock monzogranite|24196|5|Briefly described|p40|Archean|Archean|Age: 2633 +/- 2 Ma (Black et al., 2002)||||||07-NOV-08
25589|Wallsend Seam|36265|5|Briefly described|Fig.3.28|Early Permian|Early Permian|Part of the Ewington Member (Collie Coal Measures). Geological province: Collie Basin.||||||04-MAR-08
79112|Walsh Formation|63762|5|Briefly described|p19|||Contact between the diamictite and dolostone at top of unit represents the Cryogenian/Ediacaran boundary. Includes basal diamictite overlain by thinly laminated dolostone (cap carbonate). Correlates with Landrigan Fm. See also Walsh Tillite.||||||
79112|Walsh Formation|64104|6|Mentioned|p63, p70, p72|||The author proposes this name replace Walsh Tillite "to distinguish stratigraphic terms from genetic interpretation". Unconformably overlies polished and striated basement pavement .[Author has mis-spelt Edgoose as Edgegoose in bibliographic references]||||||
79112|Walsh Formation|68244|4|Described|p659-662,669-671|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. Also referred to as Walsh Tillite on 659. Discontinuously distributed throughout the Mount House and Traine River areas in west Kimberley. Glaciogenic unit deposited during of Landrigan Glaciation. Thickness at type section: c.10 m, and generally varies between 5-60m. Several Walsh Fm outcrops overlie quartzitic basement with preserved scour and chatter marks indicative of glacial scouring. Cap dolomicrite likely deposited in a low energy, deep-water environment.||Unit of Mount House Group.||Lowermost unit of Mount House Gp. Overlain by Traine Fm. Underlain by Carson Volcanics. Correlative to Landrigan Fm (Kuniandi Gp), and Mountain Valley Fm, Frank River Sst and Fargoo Fm (Duerdin Gp).|Basal diamictite: clusters of sand- to boulder-sized clasts of quartzite, dolomite, mudstone, jasper and various igneous and metamorphic rock types, siltstone-dolomicrite matrix. Overlain by thin fissile pebbly mudstone and laminated dolomicrite.|
79112|Walsh Formation|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
38971|Walsh tillite|23806|6|Mentioned|p1121|Neoproterozoic|Neoproterozoic|Informal - see Walsh Tillite.||||||
40779|Walter Williams Formation""|24494|6|Mentioned|p12|||Informal - see Walter Williams Formation.||||||
38581|Walter Williams Ultramafic Unit|23782|5|Briefly described|p8 Fig. 6|||Geological Province: Yilgarn Craton.||||||
70698|Waltha Woora Beds''|62453|6|Mentioned|p65|||Informal Name. ||||||
73786|Walwa pegmatites|50542|6|Mentioned|p97|Paleozoic|Paleozoic|||||||07-FEB-11
75107|Wambyn monzogranite|64769|6|Mentioned|p122, p122 Fig. 122|||Informal name. May just be the name of a dimension stone rather than a unit? In Western Australia.||||||21-APR-09
29110|Wanda Wanda Beds|29784|6|Mentioned|Table 1|||||||||
29110|Wanda Wanda Beds|30900|6|Mentioned|p67|||On Table 1||||||
29110|Wanda Wanda Beds|34324|6|Mentioned|p122|||See also P125 & Table||||||
29110|Wanda Wanda Beds|36869|6|Mentioned|p48|||||||||
29110|Wanda Wanda Beds|37373|6|Mentioned|Table 2.I|||||||||
29110|Wanda Wanda Beds|73391|6|Mentioned|Appendices.|||McCall (1969). Regional stratigraphic correlation chart of other workers.||||||
32884|Wandagee Beds|48848|14|Not recorded|p.54|||||||||
68081|Wandagee kimberlites|24568|5|Briefly described|p173|Jurassic|Jurassic|Informal name.  Age: 164Ma.  Geological Province: Pilbara Craton.||||||
25697|Wandarry Shale Member|40937|6|Mentioned|p28|||||||||
25697|Wandarry Shale Member|70958|4|Described|p5, p13 App. 1, Fig. 1|Paleoproterozoic|Paleoproterozoic|New name after Wandarry Creek. Said to be defined, but no type section established. At least 3000 m thick. Turee Creek sheet area, S of Ashburton River.||Of Ashburton Formation.||Basal member, overlain by Capricorn Member. Base not exposed. Overlapped by Bangemall Group in south.|Silty shale with minor fine to medium grained greywacke. Bedding hard to detect.|
75798|Wandarry supersequence|24607|5|Briefly described|p968|||Upper, mudstone-rich part of the Ashburton Formaton. Deep marine basin.||||||
72278|Wanderrie banks|61848|5|Briefly described|p301|||Sandy banks ailigned along contours, perpendicular to the sheet flow direction of sheet-wash fans.  In the region of the Harmony gold deposit.||||||
25591|Wandgee Formation|41071|6|Mentioned|p25|||Misspelling of Wandagee Formation?||||||
75967|Wandimarra Formation|64161|6|Mentioned|p592|Statherian|Statherian|Sandstone. K-Ar age of ~1688 Ma||||||
26199|Wandiwarra Formation|7161|6|Mentioned|p90, p99 Fig.9|||Earaheedy Basin. Less than 900m thick (from p99 Fig.9). Age is set by K-Ar diagenetic glauconite within this formation.|1685+/-35 Ma|||||02-MAY-12
26199|Wandiwarra Formation|7471|5|Briefly described|p8, Map Legend|Proterozoic|Proterozoic|Earaheedy Basin.||Of the Miningarra Subgroup.||Overlies Windidda Formation.|Includes stromatolitic carbonate rocks, sandstone, marine shale, and minor conglomerate.|
26199|Wandiwarra Formation|22493|6|Mentioned|p90|Statherian|Orosirian|1685+/-35Ma||||||
26199|Wandiwarra Formation|23529|5|Briefly described|p10|||Downgraded to Member status - see Wandiwarra Member of Chiall Formation.   Geological Province: Earaheedy Basin||||||
26199|Wandiwarra Formation|23588|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Underlain by Windidda Formation. Geological Province: Earaheedy Basin. Max. thickness: 1500 m.||||||07-NOV-08
26199|Wandiwarra Formation|23589|5|Briefly described|p3|||Upper sandy part and Princess Ranges Quartzite now known as Wandiwarra Member of Chiall Formation. 1688+/-72 Ma (Glauconite).  Of Miningarra Subgroup. Earaheedy Basin.||||||
26199|Wandiwarra Formation|24017|6|Mentioned|p16|||Reduced to member status - see Wandiwarra Member of Chiall Formation.||||||
26199|Wandiwarra Formation|30010|6|Mentioned|p45|||||||||
26199|Wandiwarra Formation|31217|2|Defined|p41|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
26199|Wandiwarra Formation|32727|6|Mentioned|p7|||Refers Hall & Goode (1975)||||||
26199|Wandiwarra Formation|36551|6|Mentioned|Table 29|||||||||
26199|Wandiwarra Formation|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26199|Wandiwarra Formation|37300|6|Mentioned|p81|||||||||
26199|Wandiwarra Formation|37460|3|Fully described|p142|||||||||
26199|Wandiwarra Formation|38515|4|Described|p12|||||||||
26199|Wandiwarra Formation|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26199|Wandiwarra Formation|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26199|Wandiwarra Formation|38978|3|Fully described|p164|||||||||
26199|Wandiwarra Formation|39894|5|Briefly described|p48|||Age dates. See also Fig.2.||||||
26199|Wandiwarra Formation|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26199|Wandiwarra Formation|40355|5|Briefly described|p6|||||||||
26199|Wandiwarra Formation|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26199|Wandiwarra Formation|40938|2|Defined|p41|Paleoproterozoic|Paleoproterozoic|Mention p13.||||||07-NOV-08
26199|Wandiwarra Formation|41997|6|Mentioned|p73|||||||||
26199|Wandiwarra Formation|43595|5|Briefly described|Table 3-9,p346|||||||||
26199|Wandiwarra Formation|43652|6|Mentioned|Fig.3,p381|||||||||
26199|Wandiwarra Formation|50188|6|Mentioned|p4 Fig. 2|||See also references to "Wandiwarra Formation". Superseded by Wandiwarra Member of the Chiall Formation.  This unit and Princess Ranges Quartzite are now mapped together as the Chiall Formation||||||16-JUL-08
26199|Wandiwarra Formation|50222|6|Mentioned|p329|||Superseded by Wandiwarra Member of the Chiall Formation (Miningarra Subgroup, Earaheedy Group).||||||22-JUN-04
26199|Wandiwarra Formation|64284|6|Mentioned|p59, p60 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Bunting (1986). Replaced by combination of Karri Karri Member and part of Wandiwarra Member. Geological Province: Earaheedy Basin.||||||07-FEB-11
26199|Wandiwarra Formation|64285|5|Briefly described|p66 Fig. 1|||Of Bunting (1986). Rocks incorporated into the Chiall Formation and Karri Karri Member, and unit no longer exists.||||||07-FEB-11
26199|Wandiwarra Formation|64772|6|Mentioned|p12, p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Superseded by Wandiwarra Member of the Chiall Formation.||||||07-FEB-11
26199|Wandiwarra Formation|66427|5|Briefly described|p46 Fig.4, p48, p63  |||Former name for the Wandiwarra Member (see references to that unit: p44 Tb.2, p46 Fig.4, p48, p63-64, p73).||||||
26199|Wandiwarra Formation|67855|5|Briefly described|p208 fig 3-8, p209|Paleoproterozoic|Paleoproterozoic|||Minningarra Subgroup|||Thick, extensive, green, laminated, micaceous shale.|
38136|Wandiwarra Formation ""|23529|6|Mentioned|p16|||Informal - see Wandiwarra Formation, now superseded by Wandiwarra Member.||||||
38136|Wandiwarra Formation ""|50188|5|Briefly described|p3|||Superseded by Wandiwarra Member when amalgamated along with Princess Ranges Quartzite into the Chiall Formation after it was recognised that these two units formed a single depositional package mappable as one unit.||||||16-JUL-08
41219|Wandiwarra member|50223|6|Mentioned|p346, p355|||Informal - see Wandiwarra Member.||||||
41219|Wandiwarra member|50224|6|Mentioned|p368 Tb.1|Paleoproterozoic|Paleoproterozoic|Informal name.  Of the Chiall Formation (Minningarra Subgroup).||||||07-FEB-11
33983|Wandoan Hill Formation|22547|6|Mentioned|Fig4,p25|||Geological province:  Victoria River Basin. Overlain by Stubb Formation.||||||14-NOV-06
24555|Wandy Wandy Shale|23594|6|Mentioned|p22|||Superseded. See also page 9 Fig. 6. Of Bangemall Group.||||||
24555|Wandy Wandy Shale|23746|5|Briefly described|p8 Fig 5|Proterozoic|Proterozoic|Superseded by Yandanunyah Formation.||||||
24555|Wandy Wandy Shale|37460|6|Mentioned|p173|||||||||
24555|Wandy Wandy Shale|37707|6|Mentioned|p14|||See also Table I.||||||
24555|Wandy Wandy Shale|39424|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24555|Wandy Wandy Shale|39426|2|Defined|Table 1|Mesoproterozoic|Mesoproterozoic|||||||
24555|Wandy Wandy Shale|41669|6|Mentioned|p46|||||||||
24555|Wandy Wandy Shale|43055|6|Mentioned|p27|||||||||
24555|Wandy Wandy Shale|44139|6|Mentioned|p277|||Hickman (1978), now abandoned. Rocks correlated with and now included in Waroongunyah Formation (Williams 1989).| | ||||10-SEP-12
78877|Wangarlu Formation, Upper|68223|6|Mentioned|p179 Fig.4|||Presented as Upper Wangarlu in figure.||||||
35983|Wangaru Formation|23377|6|Mentioned|p212 Fig.5||Early Cretaceous|of Vulcan Sub-basin.||||||
31145|Wangina Sandstone Formation|43495|5|Briefly described|11|||||||||
26983|Wanna beds|23858|5|Briefly described|p919|Early Permian|Cambrian|Geological Province: Officer Basin.||||||
26983|Wanna beds|36701|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
69128|Wannaway serpentinite|60622|5|Briefly described|p21|Archean|Archean|Informal name. Contains relict cuulate structures.||||||07-NOV-08
78076|Wanneroo Formation|68254|6|Mentioned|p1040, p1042|||Wanneroo Formation and Wanneroo Member used interchangeably in this paper.|||||Sandstone.|
25596|Warambi Basalt|41263|6|Mentioned|p57|||Misspelling of Warambie?||||||
80832|Warlawurra Supersuite|71088|6|Mentioned|p25|||West Musgrave region.|c. 1575 Ma|||||
80832|Warlawurra Supersuite|71618|6|Mentioned|p133|Calymmian|Statherian|Geological province: Musgrave Province. Possible source of ~1500-1800 Ma detrital zircons in the Madura Formation, Loongana Formation and Decoration Sandstone.|1607-1583 Ma|||||
25599|Warnbro Group sandstone|40349|6|Mentioned|p23|||||||||
38802|Waroonga Laterite|23929|5|Briefly described|p104|||||||||
38801|Waroonga Laterites""|23929|6|Mentioned|p104|||Informal name.  Geological Province: Yilgarn Craton.||||||
73871|Warraginee Granitoid Complex|24590|5|Briefly described|p40, p205|Archean|Archean|Predominantly grey gneisses. Age: ca.3600Ma. Geological Province: Marble Bar Domain.||||||07-FEB-11
34800|Warramboo Chert|22774|5|Briefly described|p573|||Age of unit 2798+/-8 Ma||||||
39776|Warrawadgine granitoid complex|24193|5|Briefly described|p874 Fig.1, p888|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
73581|Warrawagine Granitic Complex|63441|5|Briefly described|p30|Archean|Archean|Includes the Callina Supersuite in its structure. Age: >/-3576+/-6Ma for a migmatic trondhjemite.||||||07-FEB-11
73581|Warrawagine Granitic Complex|64580|4|Described|map legend||Paleoarchean|Undivided granitoid rock; metamorphosed.||||||15-DEC-08
73581|Warrawagine Granitic Complex|65827|6|Mentioned|p15, p16, p41|Paleoarchean||Granitic components contain inherited 3650-3550 Ma zircons indicative of ancient sialic crust; has a central c.3240 Ma intrusion.
||||||
73581|Warrawagine Granitic Complex|68035|5|Briefly described|p287, 284 Fig 1|Paleoarchean|Eoarchean|Includes enclaves of 3.66-3.58 Ga biotite tonalite gneiss within younger granodiorite and monzogranite.||||||
73581|Warrawagine Granitic Complex|69167|6|Mentioned|180057.1.pdf|||||||||
73581|Warrawagine Granitic Complex|69301|6|Mentioned|p5 Fig.3|||Northeastern part of Pilbara Craton. Includes enclaves of 3.66-3.58 Ga biotite-tonalite gneiss within post-3.50 Ga granodiorite and monzogranite.||||||
73581|Warrawagine Granitic Complex|70022|5|Briefly described|p113-114, 116-117, 119, 121|||Hosts three clusters of zircons of different Archean ages. The oldest components of the Pilbara Craton are tonalitic gneiss enclaves dated up to ~3.66 Ga. CL images.|3240 Ma.|Tambina Supersuite.||Adjacent to the Muccan Granitic Complex.|Granodiorite. Includes a banded tonalite gneiss enclave.|
36840|Warrawagine Granitoid Complex|23415|6|Mentioned|Map Legend (Simplified geol.)|||Geological province: Pilbara Craton.||||||07-JAN-08
36840|Warrawagine Granitoid Complex|23583|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|23585|4|Described|p11|Archean|Archean|Overlain by Fortescue Group. Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|23757|4|Described|p9|Archean|Archean|Probably underlies Eel Creek and Callawa Formations. Age: c.3313-3303 Ma (SHRIMP U-Pb zircon). Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|23783|5|Briefly described|p18|Archean|Archean|||||||07-NOV-08
36840|Warrawagine Granitoid Complex|23807|5|Briefly described|p111|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|23895|5|Briefly described|p884 Fig.1|||Geological Province: Pilbara Craton.||||||07-MAR-05
36840|Warrawagine Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3655-3242Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
36840|Warrawagine Granitoid Complex|24184|4|Described|p703, 706|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.3661-3570Ma||||||07-NOV-08
36840|Warrawagine Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130, p146 Tb.2-21|||See also p153 Fig.2-140. No named constituents.|||||Foliated biotite monzogranite, granodiorite, tonalite; gneiss and migmatite with greenstone xenoliths.|
36840|Warrawagine Granitoid Complex|44229|5|Briefly described|Map legend|Archean|Archean|metamorphiosed, medium- to coarse-grained monzogranite, syenogranite, granodiorite and tonalite; massive , seriate and porphyritic varieties; foliated to gneissic.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|50544|3|Fully described|p27-28, p10 Fig. 5|Archean|Archean|Mostly orthogneiss or has a gneissic or strongly foliated fabric; recrystallised and deformed with incipient to prominent mineral segregation.  Age: c.3655-3242Ma (Nelson, 1996, 1998).  Unconformably overlain by Gorge Creek Group.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|50555|5|Briefly described|Map legend|Archean|Archean|Age: 3655-3242Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
36840|Warrawagine Granitoid Complex|60429|4|Described|p6 Fig. 3, p14|||Unconformably overlain by Gorge Creek and Fortescue Groups. Geological Province: Pilbara Craton. See also p8 Fig. 4.||||||07-FEB-11
80352|Warrawagine gneiss|70775|5|Briefly described|p1|Eoarchean|Eoarchean|Informal name. This unit is the oldest rock identified in ouctrop in the Pilbara Craton. It is preserved in outcrop-scale xenoliths within Paleoarchean granodiorite.|c. 3650 Ma||||Banded tonalite gneiss.|05-FEB-18
38596|Warrawoona Group basalts|23783|6|Mentioned|p16|||Not intended as a formal name.||||||
38596|Warrawoona Group basalts|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Informal reference to undivided basalts of the Warrawoona Group. Geological Province: Pilbara Craton.||||||07-NOV-08
40531|Warrawoona Group, lower|24531|6|Mentioned|p11 Tb. 2|||Informal - see Warrawoona Group.||||||
70370|Warrawoona Group, upper|24590|6|Mentioned|p17|||Informal - see Warrawoona Group.||||||07-FEB-11
70370|Warrawoona Group, upper|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Informal name.  Includes the Antarctic Chert Member. Geological Province: Pilbara Craton.||||||07-NOV-08
29120|Warrawoona Succession|31829|6|Mentioned|p33|||||||||
40162|Warrawoona Tholeiites|24621|6|Mentioned|p79 Fig. 6|||Informal reference to tholeiitic rocks within the Warrawoona Group.||||||
40163|Warrawoona basalts|24621|5|Briefly described|p81-82|||Informal reference to the basalts within the Warrawoona Group.||||||
32960|Warrawoona schists|44297|14|Not recorded|p.13|||(F51-9).||||||
38620|Warrawoonah Group|23784|5|Briefly described|p3 Fig. 1|Archean|Archean|Misspelt - see Warrawoona Group.||||||07-NOV-08
38620|Warrawoonah Group|24185|5|Briefly described|p735 Fig.2, p751|Archean|Archean|Age: 3430-3200 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
32967|Warren River Sandstone|44303|14|Not recorded|p.9||Mesozoic|Mesozoic. (I/50-5,9).||||||
38077|Warrie Shale Member|23570|6|Mentioned|p129|||Of Jeerinah Formation.   Geological Province: Pilbara Craton||||||
81149|Warriup beds""|71789|6|Mentioned|p100|||Mention p100 to Maitland 1907. Name used by Maitland (1907) for what is now part of Pallinup Siltstone.||||||
37099|Warroo Hill member|23746|6|Mentioned|p28|||See Warroo Hill Member.||||||
38078|Warroo Member|23570|5|Briefly described|p151|||See also Warroo Hill Member.   Of the Hardey Formation.   Geological Province: Pilbara Craton||||||18-JUN-08
34999|Warrowoona Group|23046|5|Briefly described|174|||||||||
79645|Warrupura 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 201708 (porphyritic rhyolite) yielded a regression intersecting concordia curve at 1041+\-6 Ma, interpreted as the magmatic crystallization age of the rhyolite. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1051-1039 Ma (inferred)|Unit of Tjauwata Group.|||Weakly to strongly foliated, feldspar-quartz-phyric rhyolite; subvolcanic intrusion; feldspar-quartz-phyric, felsic intrusive rock; schist derived from felsic volcaniclastic rock.|
77243|Warubuyu Formation|67375|5|Briefly described|pp49-50.|Mesoproterozoic|Mesoproterozoic|A suggested name for the Warubuyu Basalt, to reflect the existence of intercalated siliclastic rocks which can be found throughout the whole stratigraphic interval.|||||Basalts, intercalated with cherty-epidotitic mudstones, light bluish-grey shales, brownish volcaniclastic siltstones, ripple cross-laminated sandstones, minor conglomerates; a laminated microbialite marker horizon.|
77243|Warubuyu Formation|67553|5|Briefly described|p51|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Nomenclature (?)proposed by this study to encapsulate the Warubuyu Basalt, an underlying unnamed sedimentary sequence, and an intercalated siliciclastic sequence with the Warubuyu Basalt. Thickness: ~250m. Includes a conspicuous light-greenish, cherty-epidotitic, laminated microbialite marker horizon.||Unit of Cassidy Group.|||Basaltic-sedimentary sequence; sedimentary rocks include cherty-epidotitic mudstones, light bluish-grey shales, brownish volcaniclastic siltstones, ripple cross-laminated sandstones, and minor conglomerates.|
75773|Watagee Formation|65548|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Of Glen Group, Youanmi Terrane, Yilgarn Craton. Schistose pelite and psammite with porphyroblasts; banded Fe-formation and Fe-banded chert, metamorphosed; felsic volcs, volcaniclastics,  metamorphosed, deeply weathered and kaolinized; mafic intrusives.||||||25-FEB-13
78320|Watchpoint Formation|68733|6|Mentioned|p190|||Western Officer Basin.||||||
69377|Weebo granodiorite|60981|5|Briefly described|p176|Archean|Archean|Informal - see Weebo Granodiorite. Geological Province: Yilgarn Craton.||||||07-NOV-08
69377|Weebo granodiorite|70020|6|Mentioned|p122|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.|2658+\-7 Ma|||||
79546|Weedy basalt""|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||||||
34918|Weegarinna Subgroup|22905|6|Mentioned|p52 Fig. 2|||Of the Bangemall Group (Chuck, 1984).  Initially incorporated into Edmund Subgroup, now part of the Edmund Group.||||||24-JAN-06
34918|Weegarinna Subgroup|24183|5|Briefly described|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin. Of the Bangemall Group.||||||
34918|Weegarinna Subgroup|24544|5|Briefly described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Superseded, in part by Edmund Group. Of Bangemall Group. Overlain by Florry Subgroup.||||||
34918|Weegarinna Subgroup|44142|6|Mentioned|p310 Tb.4-3|||Unit in proposed subdivision of Bangemall Group by Chuck (1984).||||||
34918|Weegarinna Subgroup|50225|5|Briefly described|p387 Fig. 2|||Of Chuck (1984) - equates with part of the Edmund Subgroup (Bangemall Group) of Muhling and Brakel (1985).||||||07-FEB-11
37470|Weeli Wolli basalt|24041|6|Mentioned|p493|||Formal name not intended - see Weeli Wolli Formation||||||
37471|Weeli Wolli dolerite|24041|6|Mentioned|p493|||Formal name not intended - see Weeli Wolli Formation||||||
24089|Weelumurra Beds|38776|4|Described|p39|||See also Table 1.||||||
24089|Weelumurra Beds|40987|6|Mentioned|Table 2|||||||||
24089|Weelumurra Beds|65194|5|Briefly described|p16 Fig.2.4, p100 Fig.2.24, p102|||Dark grey pyritic lacustrine clay, overlain by gravelly conglomerate and calcrete correlated with the Millstream Dolomite. Age relative to Robe Pisolite is unknown. Up to 34 m thick.||||||07-APR-16
41139|Welcome Well andesitic volcanic complex|24196|6|Mentioned|p45|||Informal - see Welcome Well Complex.||||||
35662|Weld Range Complex|23135|5|Briefly described|p279 Fig.1|||||||||
32626|Weld Range Group|46456|14|Not recorded|Not recorded|||||||||
32626|Weld Range Group|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.||Murchison Supergroup.|Kalli, Madoonga Formations.|||
32626|Weld Range Group|69584|6|Mentioned|p5 Fig.2|Mesoarchean|Mesoarchean|||Murchison Supergroup|Kalli Formation, Madoonga Formation|Overlain by the Minjar Group||
32626|Weld Range Group|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.||Murchison Supergroup.|Kalli, Madoonga Formations.|Is overlain by Minjar Group.||
39442|Weldon Creek lava member|22754|6|Mentioned|p23|||Informal unit of Camp Shale member (Koongie Park Formation).  See also Weldon Creek Lava member and Weldon Creek member.||||||
39836|Weldons Creek member|22754|5|Briefly described|p24 Fig. 5|||Misspelt - see Weldon Creek Lava Member and Weldon Creek lava member (Koongie Park Formation).  Abbreviation of one or both of these units?||||||
38721|Werillup Formation, lower|24397|5|Briefly described|p241, p236|||Superseded by North Royal Formation.  Geological Province: Eucla Basin.||||||
38727|Werillup Formation, upper|24397|5|Briefly described|p241|||Informal name no longer required.  Geological Province: Eucla Basin.||||||
74621|Werrillup Formation|64340|5|Briefly described|p26 Tb. 5, p28, p31|Late Eocene|Late Eocene|Of Eundynie Group.||||||
74621|Werrillup Formation|65194|5|Briefly described|p135, p136 Fig.4.37, p138 Fig.4.38|Middle Eocene|Early Eocene|Unconformably overlies weathered basement rocks in the Cowan Palaeovalley. Carbonaceous clay, silt and sand deposits with lignite. Norseman Limestone overlies the earlier part of this unit and is overlain by later parts.||||||
74621|Werrillup Formation|65260|6|Mentioned|p27 Fig.20|Middle Eocene|Middle Eocene|Of Eundynie Group. Fluviodeltaic to estuarine sediments; overlies North Royal Formation.||||||
78421|Werrillup Formation, Lower|65260|6|Mentioned|p26, p27 Fig.20|Middle Eocene|Middle Eocene|Of Eundynie Group. Cowan Palaeochannel. Quartz sands, clay and lignite. Proposed (by Clarke 2003) to be called North Royal Formation.||||||
78422|Werrillup Formation, Upper|65260|6|Mentioned|p27 Fig.20|Upper Eocene|Middle Eocene|Of Eundynie Group. Stratigraphy proposed by Clarke et al. (2003) names this unit Werrillup Formation.||||||
26995|Werrilup Formation|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Of Plantagenet Group. Presented as Werrilup.||||||07-FEB-11
26995|Werrilup Formation|23331|4|Described|1088||Late Eocene|||||||
26995|Werrilup Formation|23488|5|Briefly described|p40|||Equivalent to the Pidinga Formation (Eucla Basin). Geological Province: Bremer Basin.||||||28-JUL-09
26995|Werrilup Formation|23533|5|Briefly described|p561|Late Eocene|Middle Eocene|Of Plantagenet Group. Overlying unit Pallinup Formation. Geological Province: Bremer Basin.||||||
26995|Werrilup Formation|23584|5|Briefly described|p31 Fig 17|Eocene|Eocene|Of Eundynie Group. Geological Province: Eucla Basin.||||||
26995|Werrilup Formation|23768|5|Briefly described|p59|Late Eocene|Late Eocene|Contains the Nanarup Limestone Member.||||||30-MAR-05
26995|Werrilup Formation|23797|5|Briefly described|p3|||Underlies Princess Royal Spongolite. Geological Province: Yilgarn Craton.||||||15-AUG-06
26995|Werrilup Formation|23989|5|Briefly described|p54 Fig. 46|Middle Eocene|Early Eocene|Geological Province: Yilgarn Craton||||||
26995|Werrilup Formation|24557|5|Briefly described|p959 Fig.2|Middle Eocene|Middle Eocene|Geological Province: Bremer Basin.||||||11-JAN-05
26995|Werrilup Formation|32311|4|Described|p12|||||||||
26995|Werrilup Formation|32552|6|Mentioned|p70|||U.Eocene||||||
26995|Werrilup Formation|36200|6|Mentioned|p5|||||||||
26995|Werrilup Formation|40148|6|Mentioned|p161|||||||||
26995|Werrilup Formation|40877|5|Briefly described|p55|||||||||
26995|Werrilup Formation|42183|6|Mentioned|p363|||||||||
26995|Werrilup Formation|42734|5|Briefly described|map legend|Tertiary||||||||
26995|Werrilup Formation|43280|6|Mentioned|Map Legend||Tertiary|||||||
26995|Werrilup Formation|43838|4|Described|p4, Fig2 p6, 9||Tertiary|In Lefroy, Cowan & Mt Morgan Palaeodrainages. Interfingers with Norseman Limestone in Cowan Palaeod.||||||12-JUL-16
26995|Werrilup Formation|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Eocene|Eocene|Geological Province: Yilgarn Craton.||||||08-FEB-10
26995|Werrilup Formation|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|Bremer and West Eucla Basins. Age shown as Lutetian to Priabonian.||||||
26995|Werrilup Formation|69598|5|Briefly described|p2, p9, p10, p11 Tb.1, p29 Tb.4|Late Eocene|Middle Eocene|Eucla Basin. Potential carbon dioxide storage reservoir; also contains potential sealing lithologies. Deposited in non-marine to marine environments. ||Plantagenet Group||Overlain by the Pallinup Formation.|Siltstones, sandstones, claystones and brown coal.|
41471|Wesley Yard Granite|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Sally Downs Supersuite. Age: 1825Ma. Geological province: Kimberley Province.||||||07-FEB-11
41471|Wesley Yard Granite|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
68726|West Angelas Member|60706|5|Briefly described|p623 Fig.2|||Misspelt - see West Angela Member. Of the Wittenoom Formation. Geological Province: Hamersley Basin.||||||
68726|West Angelas Member|64384|5|Briefly described|p36|||Basal shale component of Wittenoom Dolomite. This shale is absent in some areas in the west of the basin. Geological province: Hamersley Basin.||||||07-FEB-11
68726|West Angelas Member|67201|6|Mentioned|p34 Fig.18|||Shown as West Angelas Mbr.||Wittenoom Formation||||25-NOV-16
68726|West Angelas Member|72493|5|Briefly described|p30|||Hamersley Basin.||Wittenoom Formation.||Overlies Mount Newman Member (Marra Mamba Iron Formation). Is overlain by Paraburdoo Member.|Shale.|
37084|West Creek formation|23723|4|Described|p36|Proterozoic|Proterozoic|Made up of Kiangi Creek Formation and Coobarra Formation. Underlying unit Gap Well formation. Geological Province: Jillawarra basin. Max. thickness: 1500 m.||||||
81585|West Dolerite|72057|6|Mentioned|p242|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||Unit of Cave Rocks Dolerite.||||
39225|West Kimberley lamproites|23897|5|Briefly described|p378|Miocene|Miocene|Informal name.||||||
41140|West Leonora basalts|24196|6|Mentioned|p69 Fig.10|||Informal - see also East Leonora basalts. Geological Province: East Agnew-Mount Clifford sub-domain, Yilgarn Craton.||||||28-MAY-04
38586|Western Granite|23782|6|Mentioned|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
38586|Western Granite|23904|5|Briefly described|p29|||Informal name.  Geological Province: Yilgarn Craton.||||||
38586|Western Granite|60667|5|Briefly described|p1126 Fig. 2, p1127|Archean|Archean|Age: 2631+/-10Ma (oldest zircons/SHRIMP).||||||07-NOV-08
80042|Western Paragneiss|67268|5|Briefly described|p8-9|||Nornalup zone. Maximum depositional age.|c. 1360 Ma||||Garnet-sillimanite migmatites and quartzites.|15-JUN-22
38587|Western Ultramafic|23782|6|Mentioned|p29 Fig. 21|||Informal name.  Geological Province: Yilgarn Craton.||||||
38587|Western Ultramafic|60514|6|Mentioned|p94, p95|Archean|Archean|Geological Province: Yilgarn Craton.Dips steeply to the west.Subaqueous intrusive sequence.||||||07-FEB-11
38587|Western Ultramafic|60628|5|Briefly described|p87, 90|||Contains well developed spinifex textured komatiites. Dips steeply to the west. Overlies Eastern Ultramafic. Local name.||||||
38587|Western Ultramafic|60629|5|Briefly described|p94 Fig.1, p95|||Dips steeply to the west. Local name. Overlies Eastern Ultramafic. See also Western Ultramafic unit.||||||
38587|Western Ultramafic|69414|5|Briefly described|p89-93, 100-103|Archean|Archean|Yilgarn Craton. Not part of the Agnew-Wiluna Greenstone belt. Cosmos mine succession, 5-100m thick. Unmineralised.|Between 2736 Ma and 2730 Ma.||||Effusive komatiite eruptions: olivine mesocumulates and orthocumulates, which have undergone pervasive serpentinisation obscuring the primary cumulate textures.|
38594|Western Ultramafic Unit|23782|4|Described|p54|||Informal name.  Geological Province: Yilgarn Craton.||||||
38594|Western Ultramafic Unit|69617|6|Mentioned|p154|||Deposition wass coeval with deposition of Honman Formation.||||||
38594|Western Ultramafic Unit|73596|6|Mentioned|p1156, 1169|Neoarchean|Neoarchean|Kathleen Valley Domain, Agnew-Wiluna Greenstone Belt.|c.2730 Ma.|||Is overlain by Cosmos Komatiite.||
69130|Western Ultramafic unit|60628|6|Mentioned|p89 Fig.2|||Local name. See also Western Ultramafic.||||||
69130|Western Ultramafic unit|60629|5|Briefly described|p94, 95|||Well developed spinifex textures. Dips steeply to the west. Subaqueous extrusives. Local name. See also Western Ultramafic.||||||
69130|Western Ultramafic unit|60630|6|Mentioned|p115|||||||||06-JUN-05
36762|Westonia diorite|23773|5|Briefly described|p753||Mesoproterozoic|Age: 1215+/-11 Ma. Yilgarn Craton.||||||
35009|Whaleback Member|23045|5|Briefly described|289|||Of Brockman Iron Formation.||||||
29136|Wheat Belt Granite""|40359|6|Mentioned|p11|||Informal name||||||
29136|Wheat Belt Granite""|40370|6|Mentioned|p9|||||||||
37203|Whim Creek Group""|23793|6|Mentioned|p6|||Informal||||||
37203|Whim Creek Group""|24140|6|Mentioned|p217 Fig. 2|||Informal - see Whim Creek Group.||||||
25618|Whim Creek argillites""|36551|6|Mentioned|p59|||||||||
69728|Whim Creek group|24140|6|Mentioned|p217 Fig. 2, p229|||Informal - see Whim Creek Group.||||||
27931|Whim Creek slate|32189|4|Described|p197|||||||||
27931|Whim Creek slate|39697|6|Mentioned|p106|||||||||
81990|White Flag Formation, Lower|72814|5|Briefly described|p201, Fig. 3, p202 Fig. 4|||West of Zuleika Shear, Coolgardie Domain.|||||Sandstone, siltstone and shale.|
81990|White Flag Formation, Lower|73391|5|Briefly described|p194, 244-245|||Coolgardie, Ora Banda Domains, Kalgoorlie Terrane.||||Overlies Talbot formation, locally unconformably. Is overlain by Upper White Flag Formation.|Mostly conglomerate derived mainly from an andesitic volcanic source.|
81989|White Flag Formation, Upper|72814|6|Mentioned|p201, Fig. 3|||Seems to be the same as White Flag Formation of Fig.4.||||||
81989|White Flag Formation, Upper|73391|5|Briefly described|p194-195, 244-245, Appendices.|||Coolgardie, Ora Banda Domains, Kalgoorlie Terrane.||||Overlies Lower White Flag Formation. Is overlain by Gibson-Honman formation (Lower Black Flag Formation).|Mainly juvenile andesitic volcanic rocks: andesitic tuff breccia and tuffs, minor dolerite sills.|
29484|White Hill Road Member|63454|5|Briefly described|p71 Tb. 2|||Abbreviated version of White Hill Limestone Member - used interchangeably in article.||||||13-AUG-07
77568|White Hills Supersequence|66937|5|Briefly described|p155, pp166-168.|Archean|Archean|Kalgoorlie Terrane. Lake Carey Basin. Poorly exposed. Lithofacies stacking is aggradational.||||Unconformably overlies, and is thrust interleaved with, Laverton Sequence. Is unconformably overlain by Brock Supersequence.|Sequences of uniform associations of graded massive fine- to very fine-grained sandstone, siltstone and black shale with bedded chert.|
77568|White Hills Supersequence|66938|6|Mentioned|p187. |Archean|Archean|||||||
83073|White Hope Basaltic Andesite|73151|6|Mentioned|p12|||Misspelling of White Hope Basalt?||||||
25619|White Lake conglomerate|30219|6|Mentioned|p218|||Should be White Lake metaconglomerate||||||
80621|White Polyzoal Limestone""|65942|6|Mentioned|p74|||Of Tate (1879).||||||
32550|Whitestones Series|45310|14|Not recorded|p.33.|||Younger Precambrian.||||||
31147|Wicherina Beds|23279|6|Mentioned|p11|||(McKellar, 1972).||||||
31147|Wicherina Beds|43495|5|Briefly described|5|||||||||
35634|Wicherina Member|23279|5|Briefly described|p11-2|||||||||
35634|Wicherina Member|23520|5|Briefly described|p11 Fig. 7|Asselian|Asselian|Geological Province: Perth Basin.||||||
35634|Wicherina Member|24410|5|Briefly described|p41|Permian|Permian|A white sandstone with minor conglomerate-filled channels and carbonaceous stringers. Geological Province: northern Perth Basin.||||||
35634|Wicherina Member|62113|3|Fully described|pp618-619, pp622-624, p630.     |Carboniferous|Carboniferous|Wicherina Beds of McKellar (1972); informally named as Member in this text. Multistorey channels within Nangetty Formation filled with coarse-grained gravity-flow facies deposited on a marine fan-delta; glacially-influenced; includes large outsized boulders. Slumping and folding typical. Palaeocurrents predominantly to the north. Possible reservoir facies for hydrocarbons.||Unit in Nangetty Formation.||Interfingers with the Nangetty Formation.|Channelized sandstone-conglomerate association. Coarse grained, with a distinctive white colour produced by kaolinization.|
35634|Wicherina Member|64635|5|Briefly described|p4 Fig.3,p17,  |Carboniferous|Carboniferous|Of Mory and Iasky (1996).||Unit in Nangetty Formation.|||Massive, rippled, contorted and pebbly sandstone facies.|
35634|Wicherina Member|67340|6|Mentioned|p6|Carboniferous|Carboniferous|Northern Perth Basin.||Nangetty Formation.||||
35634|Wicherina Member|67354|5|Briefly described|p88, p107.|||Suggested as an analogue for the depositional environment of turbidite sandstones in the Treachery Formation.||Unit in Nangetty Formation.||||
35634|Wicherina Member|70097|5|Briefly described|p20 Fig.4|Asselian|Gzhelian|Northern Perth Basin. Irwin Terrace and Dongara Saddle.||Nangetty Formation|||Sandstone.|
35634|Wicherina Member|73623|5|Briefly described|p3|Carboniferous|Carboniferous|Northern Irwin Basin and contiguous Coolcalalaya Sub-basin. Assigned to the Nangetty Formation by Eyles et al. (2006).|||||Fluvial deposits.|
40266|Widgemooltha dyke suite|23914|6|Mentioned|p159|||Geological Province: Yilgarn Craton.||||||
78423|Widgiemooltha Dyke|65260|6|Mentioned|p6 Table 1|Siderian|Siderian|Lake Cowan. Part of Widgiemooltha Dyke Suite. c.2420 Ma (Nemchin and Pidgeon 1998).||||||
33877|Widgiemooltha Dyke Suite""|22534|6|Mentioned|p26|||||||||
33877|Widgiemooltha Dyke Suite""|63253|5|Briefly described|126|||Of Sofoulis (1966)||||||
33877|Widgiemooltha Dyke Suite""|68066|6|Mentioned|p34|Proterozoic|Proterozoic|Sofoulis (1966) introduced the term for the generally east-west dykes of the Eastern Goldfields. See Widgiemooltha dyke swarm.||||||
82965|Widgiemooltha Dyke Swarm|73238|6|Mentioned|p22|||Kurnalpi Terrane.|||Binneringie Dyke.|||
27002|Widgiemooltha Monzogranite|24223|5|Briefly described|Map legend|Archean|Archean|Foliated porphyritic monzogranite.||||||07-NOV-08
27002|Widgiemooltha Monzogranite|41771|5|Briefly described|p29|||See also P31||||||
27002|Widgiemooltha Monzogranite|42221|6|Mentioned|p24|||||||||
27002|Widgiemooltha Monzogranite|42724|5|Briefly described|map legend|Archean||||||||07-NOV-08
27002|Widgiemooltha Monzogranite|42817|5|Briefly described|p18|||||||||
27002|Widgiemooltha Monzogranite|42937|5|Briefly described|p568|||||||||
27002|Widgiemooltha Monzogranite|43102|5|Briefly described|Fig.3|||||||||
27002|Widgiemooltha Monzogranite|60076|5|Briefly described|p23, p46 App. 1|Archean|Archean|[Agmwi]   Foliated porphyritic monzogranite; microcline porphyroclasts.||||||07-NOV-08
27002|Widgiemooltha Monzogranite|65264|5|Briefly described|p48 Appdx. 1|Archean|Archean|Foliated porphyritic monzogranite; microcline porphyroclasts.||||||07-FEB-11
80944|Widgiemooltha Sandstone|72049|5|Briefly described|p256|||Detrital zircon geochronology shows bi-modal age populations of 2687 +/- 8 Ma and 2731 +/- 9 Ma with the oldest grains dated at 3378 +/- 6 Ma and 3627 +/- 8 Ma. (Kositcin et al 2008).||||||18-MAR-19
79233|Widgiemooltha Supersuite|70133|5|Briefly described|Map legend|Proterozoic|Proterozoic||||Binneringie Dyke.||Dolerite and gabbro; includes cumulate and granophyric differentiates (section only).|
79233|Widgiemooltha Supersuite|70140|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||c.2410 Ma.||||Dolerite.|
79233|Widgiemooltha Supersuite|70153|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Widgiemooltha Large Igneous Province.|2420 - 2400 Ma (inferred).||||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
79233|Widgiemooltha Supersuite|70156|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Of Widgiemooltha Large Igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420-2400 Ma). Samples GSWA 207518.1 and 207518.2 (gabbro dykes) both yielded interpreted igneous crystallisation ages of 2405+\-4 Ma (weighted mean 207Pb*/206Pb*). See 500k_interpgeop14_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv.|2420-200 Ma (inferred)||Includes Binneringie Dyke, Jimberlana Norite.||Dolerite and gabbro; includes cumulate and granophyric differentiates|
79233|Widgiemooltha Supersuite|70773|6|Mentioned|p65||||c. 2410 Ma||Includes the King of the Hills Dolerite.|||
79233|Widgiemooltha Supersuite|70794|5|Briefly described|500k_interpgeop14_lut.csv,|Paleoproterozoic|Paleoproterozoic|Widgiemooltha Large Igneous Province. See 207518.1.pdf for data on dating of baddeleyite from a gabbro dyke. See 207518.2.pdf for dating of zircons. Mean igneous crystallisation age of 2405 +/- 4 Ma interpreted. Also 100k_interpgeop_lut.csv ,2_5m_interpdykel15_lut.csv,  500k_interpgeol_lut.csv, 100k_geologyp_lut.csv . |2420-2400 Ma inferred||Includes Jimberlana Norite, Binneringie Dyke.||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
79233|Widgiemooltha Supersuite|70796|5|Briefly described|2_5m_interpdykel15_lut.csv|Paleoproterozoic|Paleoproterozoic|Widgiemooltha Large Igneous Province. See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, Youanmi100_2640_stratig.pdf.|ca 2420 to 2400 Ma (inferred)||||Dolerite and gabbro; includes cumulate and granophyric differentiates|
79233|Widgiemooltha Supersuite|70802|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Yilgarn Craton, West Australian Craton. Of Widgiemooltha Large Igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420-2400 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv, 100k_geologysub10_lut.csv, 2_5m_interpdykel15_lut.csv.|2420-2400 Ma (inferred)||Includes Jimberlana Norite.||Dolerite and gabbro; includes cumulate and granophyric differentiates|
79233|Widgiemooltha Supersuite|70826|6|Mentioned|p14 tbl 5|Siderian|Siderian|Yilgarn Craton.|2420-2400 Ma|||||
79233|Widgiemooltha Supersuite|71148|6|Mentioned|p123|||Kalgoorlie Terrane, Yilgarn Craton.|||||Dolerite/gabbro dykes.|
79233|Widgiemooltha Supersuite|71269|5|Briefly described|GEOL_LUT_CSV files|Siderian|Siderian|Of Widgiemooltha Large igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420 - 2400 Ma). See 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|2420-2400 Ma||||Dolerite|
79233|Widgiemooltha Supersuite|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of the Widgiemooltha Large Igneous Province. Events: Widgiemooltha Supersuite Magmatic Event (2420 - 2400 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv. See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|2420-2400 Ma (inferred)||Includes Ballona Dolerite, Kalpini Dolerite, King of the Hills Dolerite.||Dolerite and gabbro; includes cumulate and granophyric differentiates|
79233|Widgiemooltha Supersuite|71493|5|Briefly described|p42|Siderian|Siderian|Yilgarn Craton, Eastern Goldfields Superterrane. Crystallisation age from Nemchin and Pidgeon, (1998).|2418+/-3 Ma U-Pb baddeleyite|||||
79233|Widgiemooltha Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic||||Includes Binneringie Dyke, Jimberlana Norite.||Dolerite and gabbro; includes cumulate and granophyric differentiates.|
79233|Widgiemooltha Supersuite|73056|6|Mentioned|p293 Fig.2|Siderian|Siderian|Discussed p292 as Widgemooltha dyke swarm, Widgiemoolta dykes.|2410 Ma|||||
79233|Widgiemooltha Supersuite|73057|6|Mentioned|p1-2, p4, p6|Siderian|Siderian|Yilgarn Craton. E-W to NE-SW trending dykes, up to 3.2km wide and up to 700km long. Largest intrusions show well-developed igneous layering (Jimberlana, Binneringie). Widgiemooltha dykes and Widgiemooltha dyke swarm also used.|2418-2408 Ma, 2408-2401 Ma||Eraynia dykes||Mafic dykes.|
83392|Widgiemooltha Tonalite|73391|6|Mentioned|p436|||Southern end of the Eastern Goldfields Province.|2796 +/- 31 Ma (Hill et al., 1993).|||||
77658|Widgiemooltha dyke swarm|24165|5|Briefly described|p13, Plate 1|Paleoproterozoic|Paleoproterozoic||c.2400 Ma.||||Dolerite dyke, sill and plug.|
77658|Widgiemooltha dyke swarm|63253|5|Briefly described|126|||[new name. It is implied that this name replaces Widgiemooltha Dyke Suite.]. E-W dykes generally 10-50 m thick. Sub-vertical or steeply S dipping.  Tens to hundreds of km long.|||||Massive olivine dolerite or gabbro.|30-APR-15
77658|Widgiemooltha dyke swarm|65260|6|Mentioned|p5|Siderian|Siderian|Of Nemchin and Pidgeon (1998). Subsequently Widgiemooltha Dyke Suite.||||||
77658|Widgiemooltha dyke swarm|68066|6|Mentioned|pp33-34|Proterozoic|Proterozoic|Name used by Myers (1990) for consistency with other groupings of dykes in Western Australia. See Widgiemooltha Dyke Suite"".|||Includes Binneringie and Jimberlana Dykes.|||
77658|Widgiemooltha dyke swarm|68471|6|Mentioned|p11-12, 14-17, 19|||Yilgarn Craton. Unaltered by significant metamorphic events since their formation. Palaeomagnetic declinations and inclinations tabulated.|~2.41 Ga.||||Picrite, olivine-dolerite and quartz-dolerite dykes.|
77658|Widgiemooltha dyke swarm|69404|6|Mentioned|p22|Proterozoic|Proterozoic|||||||
77658|Widgiemooltha dyke swarm|70017|6|Mentioned|p222-224, 227-230|Paleoproterozoic|Paleoproterozoic|Yilgarn Craton. Extends E-W. Siderian age. Paleomagnetic directions are relatively close to those of the Fraser dyke swarm (angular difference is 28 degrees).|2418-2410 Ma.|||||
77658|Widgiemooltha dyke swarm|73056|6|Mentioned|p292|Siderian|Siderian|Yilgarn Craton. E- to NE- trending dyke swarm. Dykes are up to 3.2 km wide, extend up to 700 km, largest intrusions (Jimberlana, Binneringie) show well-developed igneous layering. Dykes show dual magnetic polarity, emplacement may have involved several pulses. See also Widgiemoolta dykes, Widgiemoolta Supersuite.|2418-2408 Ma||||Mafic dykes.|
83186|Widgiemooltha dykes|73057|6|Mentioned|p6, p8 Fig.7, p9|Siderian|Siderian|Yilgarn Craton. E- to ENE-trending dykes. See also Widgiemooltha Supersuite, Widgiemooltha dyke swarm.|ca. 2408 Ma||Binneringie Dyke, Jimberlana Dyke|||
40356|Widgiemooltha suite|23922|5|Briefly described|p1252|Siderian|Siderian|Informal. Geological Province: Yilgarn Craton.||||||
40356|Widgiemooltha suite|50542|6|Mentioned|p123|Proterozic|Proterozoic|Informal name. Gabbro-dolerite dykes. Geological Province: Yilgarn Craton.||||||07-FEB-11
40356|Widgiemooltha suite|70281|5|Briefly described|p454, 471|||Hallberg (1987). Occurs throughout the Yilgarn Craton.|2.4 Ga.||Binneringie, Jimberlana intrusions.||Norite and gabbro dykes.|
40356|Widgiemooltha suite|70292|5|Briefly described|p339|Siderian|Siderian||2400 Ma||||Gabbro dykes.|
77785|Wild Dog Creek intrusion|60498|5|Briefly described|p1016 Fig.1, p1017.|Paleoproterozoic|Paleoproterozoic|No lithology was stated for the stratigraphic name, except for the caption referring to 'mafic-ultramafic intrusions'. Halls Creek Orogen. The correct name is Wild Dog Creek Gabbro. Intrusions form gently dipping sheets.|||||Large homogeneous gabbroic sills: magnetite gabbro, biotite gabbro, diorite.|
77785|Wild Dog Creek intrusion|69003|6|Mentioned|p22|Paleoproterozoic|Paleoproterozoic|E Kimberley region, Halls Creek Orogen. Mafic sheet-like body.||||||
78453|Wilina Pluton|65827|6|Mentioned|p22, p59|Paleoarchean|Paleoarchean|Former name of Wilina Granodiorite.
||||||
41440|Wilki Gneiss|50436|6|Mentioned|p4.2|||Superseded by Hansens Folly Granite.||||||
80323|Wilki Granite|67202|6|Mentioned|p189-p190|Neoproterozoic|Neoproterozoic|A unit in the Mount Crofton group of granites (a subdivision of the O'Callaghans Supersuite by Goellnicht et al., 1991); assigned to the O'Callaghans Suite by Wyborn (1997) and Budd et al. (2001).|within the ~655-615 Ma span.|||||15-FEB-18
27060|Wilki Quartzite|23758|6|Mentioned|p8 table 2|||Replaced by Wilki Formation.||||||
27060|Wilki Quartzite|23900|4|Described|p1537 Fig. 2|Proterozoic|Proterozoic|Of the Lamil Group. Overlies the Puntapunta Formation. Geological Province: Paterson orogen.||||||
27060|Wilki Quartzite|24194|5|Briefly described|p900 Fig.3|Neoproterozoic|Neoproterozoic|Quartzite and minor shale. Parent: Lamil Group. Geological Province: Paterson Orogeny||||||
27060|Wilki Quartzite|36551|6|Mentioned|Table 22|||||||||
27060|Wilki Quartzite|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27060|Wilki Quartzite|37212|6|Mentioned|Table 1|||||||||
27060|Wilki Quartzite|37460|4|Described|Table3.VII|||||||||
27060|Wilki Quartzite|37707|6|Mentioned|Table I|||||||||
27060|Wilki Quartzite|43278|5|Briefly described|p346,Fig.2.|Neoproterozoic|Neoproterozoic|of Yeneena Group.||||||
27060|Wilki Quartzite|43862|5|Briefly described|Fig.2 p378|||||||||
27060|Wilki Quartzite|43868|5|Briefly described|Fig.3 p154|||||||||
27060|Wilki Quartzite|44139|5|Briefly described|p277-282|Neoproterozoic|Neoproterozoic|Chin et al. (1982). 1000 m. Quartzite; minor shale, siltstone. Northeastern zone of Yeneena Basin, conformably overlies Puntapunta Formation, conformably overlain by Kaliranu beds.| | ||||06-MAR-18
27060|Wilki Quartzite|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
27060|Wilki Quartzite|62453|6|Mentioned|p69|||||||||
27060|Wilki Quartzite|65826|6|Mentioned|p13.|||Named by Chin et al. (1982). About 1.4 km thick.||||||
26215|Wilkinson Range Beds|29681|6|Mentioned|p191|||Permian||||||
26215|Wilkinson Range Beds|30012|6|Mentioned|p17|||Out dated name||||||
26215|Wilkinson Range Beds|30952|6|Mentioned|Map legend|Early Permian|Early Permian|Prob.Lower Permian||||||
26215|Wilkinson Range Beds|30965|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
26215|Wilkinson Range Beds|31092|6|Mentioned|p4|||||||||
26215|Wilkinson Range Beds|31562|4|Described|p9|||||||||
26215|Wilkinson Range Beds|31906|4|Described|p4|||L. Permian. Table 1||||||
26215|Wilkinson Range Beds|32552|2|Defined|p10|Early Permian|Early Permian|See also P37,42-46,49 etc.||||||
26215|Wilkinson Range Beds|32648|6|Mentioned|p32|||Sakmarian||||||
26215|Wilkinson Range Beds|33586|6|Mentioned|p13|||Refers Talbot & Clarke (1918).||||||
26215|Wilkinson Range Beds|33591|6|Mentioned|p9|||||||||
26215|Wilkinson Range Beds|33595|6|Mentioned|p6|||||||||
26215|Wilkinson Range Beds|33850|4|Described|Table 2|||Mention P7.||||||
26215|Wilkinson Range Beds|35496|6|Mentioned|p19|||||||||
26215|Wilkinson Range Beds|37916|6|Mentioned|p464|||Renamed Paterson Formation.||||||
26215|Wilkinson Range Beds|43593|5|Briefly described|p4||Permian|||||||
26215|Wilkinson Range Beds|46316|4|Described|p.14|Cretaceous|Permian|Map, p.5,13, Tb.1, opposite p.6. Correlated with Cretaceous & Permian beds on H51-14. Upper section is U.Jur.-L.Cret.||||||
26215|Wilkinson Range Beds|60076|6|Mentioned|p32|Permian|Permian|||||||
26215|Wilkinson Range Beds|65264|5|Briefly described|p27|Permian|Permian|Overlies the Officer Basin.||||||07-FEB-11
83335|Wilkinson Range Series/Beds''|73117|6|Mentioned|p26|||(Talbot et al., 1917; Talbot and Clarke, 1917; Lowry, 1970). [Written as 'Wilkinson Range Series/Beds']. A now-informal unit partly incorporated in the Paterson Formation.||||||
31340|Williambury Sandstone|12733|6|Mentioned|p554 Fig.2.|Early Carboniferous|Early Carboniferous|Tournaisian-Visean.||||Overlies Moogooree Limestone. Is overlain by Yindagindy Formation.||
31340|Williambury Sandstone|43566|6|Mentioned|Fig.3,p416|||||||||
31340|Williambury Sandstone|60725|5|Briefly described|p29 Fig.2, p30, p36 Fig.6. |Carboniferous|Carboniferous|||||||
31340|Williambury Sandstone|69029|6|Mentioned|p326|Visean|Tournasian|Of onshore Carnarvon Basin.||||Overlain by Yindagindy Formation. Underlain by Moogooree Limestone.||
30633|Williambury granodiorite|69166|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic||1672 Ma +/-18 Ma (SHRIMP)||||Medium grained granite.|
70613|Williamstown Cherts|62406|5|Briefly described|p54 Fig. 2|||This name probably refers to a part of the Williamstown Dolerite and was not intended as a formal name.||||||
41090|Williamstown dolerite|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain.  Of the Kalgoorlie Group.  Age: 2691 +/- 6Ma (zircon).||||||07-NOV-08
83933|Williamstown gabbro|70290|5|Briefly described|p296-298|||Kalgoorlie district, Yilgarn Craton. U-Pb zircon SHRIMP date.|2696 +/- 5 Ma (U-Pb; Fletcher et al., 2001).|||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.|Gabbro sill. Greenschist facies metamorphism.|
39342|Williamstown peridotite|24091|4|Described|p44|Archean|Archean|Informal name. KANOWNA 1:100 000. Age: 2696+/-5Ma (Pb/Pb). Geological Province: Yilgarn Craton. Maximum Thickness: 300m||||||07-NOV-08
75506|Williespe Formation|64630|5|Briefly described|p31 Fig.2|Guadalupian|Roadian|Province: Southern Perth Basin. Overlies the Redgate Coal Measures. Palynology age: D. ericianus to D. parvithola. Base correlates with base of Muja Coal Measures.||||||12-SEP-13
42434|Wilson Bluff Limestone calcareous marl|24557|6|Mentioned|p959|||Informal reference to marl within the Wilson Bluff Limestone. See also Wilson Bluff marl and Wilson Bluff bryozoan marl.||||||
42436|Wilson Bluff bryozoan marl|24557|6|Mentioned|p961|||Informal reference to marl within the Wilson Bluff Limestone. See also Wilson Bluff marl and Wilson Bluff Limestone calcareous marl.||||||11-JAN-05
42435|Wilson Bluff marl|24557|6|Mentioned|p960|||Informal reference to marl within the Wilson Bluff Limestone. See also Wilson Bluff Limestone calcareous marl and Wilson Bluff bryozoan marl.||||||11-JAN-05
70642|Wilson Well suite|61252|6|Mentioned|p67 Tb.1|||Informal name. Of the Carlindi granitoid complex.||||||
79826|Wilson's Bluff Formation|69632|5|Briefly described|p21 Tb.6, p26, p30, p32|Eocene|Eocene|Gunbarrel, Eucla Basins. Approx. 71m thick in drillhole FOR004. Average shear-wave velocities tabulated.||||Overlies Hampton Sandstone.|White to grey, soft, poorly lithified cool-water chalk, limestone.|
38723|Wilson's Bluff Limestone|24397|6|Mentioned|p237|||Of Singleton (1954). Superseded by Wilson Bluff Limestone.  Geological Province: Eucla Basin.||||||19-FEB-15
38723|Wilson's Bluff Limestone|65942|6|Mentioned|p75|||||||||
38723|Wilson's Bluff Limestone|69386|5|Briefly described|p7|Eocene|Eocene|Eucla Basin.||||Is overlain by Abrakurrie Limestone.|Soft, poorly lithified cool-water carbonate.|
31377|Wilsons Cliff Sandstone|43563|6|Mentioned|p4|||||||||
34578|Wilsons Cliffs Sandstone|22753|5|Briefly described|Fig.3 p585|Ordovician|Ordovician|||||||
34578|Wilsons Cliffs Sandstone|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins.||||Conformably underlies Goldwyer and Nita Formations and laterally equivalent to Willara Formation. Unconformably overlies Nambeet Formation.|Includes sandstone.|
24576|Wilthorpe Conglomerate|22694|6|Mentioned|p7|||||||||
24576|Wilthorpe Conglomerate|23744|6|Mentioned|p15|||Renamed Wilthorpe Formation.||||||
24576|Wilthorpe Conglomerate|23747|6|Mentioned|p14|||See Wilthorpe Formation.||||||
24576|Wilthorpe Conglomerate|35975|2|Defined|p103|Proterozoic|Proterozoic|||||||
24576|Wilthorpe Conglomerate|40989|4|Described|p26|||||||||
24576|Wilthorpe Conglomerate|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Superseded by Wilthorpe Member of Labouchere Formation (Windh 1992); now Wilthorpe Formation of the Padbury Group.||||||
24576|Wilthorpe Conglomerate|65419|5|Briefly described|p37, pp40-41.|Paleoproterozoic|Paleoproterozoic|Of Gee (1979, 1987); the Wilthorpe member of Windh (1992); later the Wilthorpe Formation of Martin (1994, in prep.).||Formerly a unit in Padbury Group.||||04-NOV-13
24576|Wilthorpe Conglomerate|67855|5|Briefly described|p206|||Up to 3 km thick. Fluvial deposit. Clasts: vein quartz, ferruginous and silica-cemented quartz sandstone, jasper and chert, probably derived from Glengarry Formation.||Padbury Group||Overlies Glengarry Group. Overlain by Robinson Range Formation.|Boulders to 2m across. Lenses of bouldery and pebbly conglomerate in gritty pebbly sandstone showing imbrication and festoon cross-bedding.|
36366|Wilthorpe Conglomerate""|22940|6|Mentioned|p17|||Superseded by Wilthorpe Formation.||||||29-OCT-15
72831|Wilthorpe Member|49896|5|Briefly described|p3 Tb. 2|||Interpreted as part of Labouchere Formation by Windh (1992); formerly called Wilthorpe Conglomerate - now superseded by Wilthorpe Formation.||||||
37092|Wilthorpe granite|23744|6|Mentioned|p6|||Informal and superseded by Despair Granite.||||||
35523|Wilthorpe granite""|22940|6|Mentioned|p5|||Informal - superseded by Despair Granite.||||||
83155|Wiluna Group|72491|6|Mentioned|p5 Fig.4|||Kalgoorlie Terrane, Yilgarn Craton. Appears as Wiluna Gp.||||||
42468|Wiluna chromites|60696|6|Mentioned|p344 Fig. 2|||Informal name.||||||
73600|Wiluna komatiites|63459|5|Briefly described|p814|Archean|Archean|Not intended as a formal name. Relict pyroxene, plagioclase and amphibole and chromite crystals are well preserved, whereas former olivine grains are entirely serpentinised. Geological Province: Yilgarn Craton.||||||07-NOV-08
35719|Winburn Suite|24197|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Composed of charnockites, rapakivi, megacrystic and biotite granites. Possibly derived from same magmatic episode as Giles Complex. Together with Kulgera Supersuite intrudes Birksgate Complex. Age: 1080Ma. Geol.Prov: Musgrave Block. Eg.of Sybella Assocn.||||||07-FEB-11
35719|Winburn Suite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1200Ma.||||||09-MAY-05
35719|Winburn Suite|50607|5|Briefly described|p1.1, 3.1|Mesoproterozoic|Mesoproterozoic|Age: ~1550-1080Ma. Geological Province: Musgrave Block.||||||
35719|Winburn Suite|71268|5|Briefly described|1m_geologyp12_lut.csv|||Kirkland et al. (2010) reported a U-Pb zircon crystallisation age of 1077+\-6 Ma.|||Includes Winburn Granite.|||
79629|Winburn granite|68996|5|Briefly described|p7, 34, 39, 47, 50, 52,57, p61,62,64,65|Mesoproterozoic|Mesoproterozoic|6km thick. Large (~4500 km3) stratiform intrusion.|1077+/-6 Ma U/Pb SHRIMP|Giles Suite, Warakurna Supersuite||Sits above the Jameson intrusion.|Granites.|
79629|Winburn granite|71211|6|Mentioned|p10-p11, p216, p219, p234|||Informal name. |||||Rapakivi monzogranite to alkali-feldspar granites and quartz-alkali feldspar syenites.|
29152|Windalia Formation|30875|6|Mentioned|p10|||See also P13. Aptian-Albian age||||||
29152|Windalia Formation|31604|5|Briefly described|p6|||See also Table 4. Albian. Unit of Winning Gp.||||||
29152|Windalia Formation|32712|6|Mentioned|Table 1|||||||||
29152|Windalia Formation|32715|6|Mentioned|Fig.16|||||||||
29152|Windalia Formation|34472|6|Mentioned|p1812|||Table. See also P1815||||||
29152|Windalia Formation|36331|6|Mentioned|p5|||||||||
29152|Windalia Formation|36751|6|Mentioned|p449|||||||||
29152|Windalia Formation|63068|5|Briefly described|p44 Fig. 2|Aptian|Aptian|Of the Winning Group. Underlies Gearle Limestone. Geological Province: Carnarvon Basin.||||||27-FEB-07
42395|Windalia Sands""|23815|6|Mentioned|p296|||Uppermost unit of Muderong Shale.||||||
29153|Windalia sands|38655|6|Mentioned|p8|||||||||
29153|Windalia sands|42677|6|Mentioned|p18|||||||||
29153|Windalia sands|44870|14|Not recorded|p221||Early Cretaceous|SF50-1 (Barrow Island)||||||
76207|Windanning Formation|67056|6|Mentioned|p429. |||Yalgoo-Singleton Greenstone Belt. Hosts the supergene martite-goethite Mungada deposits.||||||
76207|Windanning Formation|69267|5|Briefly described|p651-654|||Murchison Province, Yilgarn Craton.|3050-2950 Ma.|Luke Creek Group.|Mount Gibson banded iron formation.|Overlies Gabanintha Formation.|A succession of BIF and chert interlayered with felsic volcaniclastic and volcanogenic rocks and minor basalt.|
25633|Windara Granite|35113|6|Mentioned|p52|||||||||
81554|Windida Member|71484|6|Mentioned|p125|||Misspelt, see Windidda Member p131-132.||||||30-AUG-19
41220|Windidda formation|50223|6|Mentioned|p346|||Informal - see Windidda Formation.||||||
27936|Windimurra Complex|22556|4|Described|p555||Archean|Divided into and described as Shephards Discordant Zone and Canegrass Magnetite Zone throughout text.||||||07-NOV-08
27936|Windimurra Complex|23159|5|Briefly described|table3|Archean|Archean|||||||07-NOV-08
27936|Windimurra Complex|23787|4|Described|p68|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
27936|Windimurra Complex|23922|5|Briefly described|p1234|Archean|Archean|Geological Province: Yilgarn Craton.  Age: 2.80 +/- 0.04 Ga (Sm-Nd mineral isochron).||||||07-NOV-08
27936|Windimurra Complex|24160|6|Mentioned|p73|||||||||
27936|Windimurra Complex|31222|6|Mentioned|p9|||||||||
27936|Windimurra Complex|33848|6|Mentioned|p53|||Refers de la Hunty(1970).||||||
27936|Windimurra Complex|35468|6|Mentioned|p20|||||||||
27936|Windimurra Complex|35469|6|Mentioned|p45|||Also shown on Fig.9||||||
27936|Windimurra Complex|37795|6|Mentioned|p179|||||||||
27936|Windimurra Complex|38492|4|Described|p17|||See also p7.||||||28-OCT-08
27936|Windimurra Complex|40337|4|Described|p12|||||||||
27936|Windimurra Complex|41040|4|Described|p1196|||||||||
27936|Windimurra Complex|41678|6|Mentioned|p30|||||||||
27936|Windimurra Complex|42010|4|Described|p172|||||||||
27936|Windimurra Complex|42019|6|Mentioned|p23|||||||||
27936|Windimurra Complex|42978|4|Described|p281|||see also Fig.1,p282||||||
27936|Windimurra Complex|44149|4|Described|p13, p60, p69, p72 Fig.2-83, p119-124 |Neoarchean|Mesoarchean|Largest single body of gabbroid rocks in the Yilgarn Craton. Made of 13.5km thick layered series and a Border Group of altered and deformed gabbro. Appears as Windimurra Mafic Complex in Fig.2-75. Sm-Nd two-point whole-rock isochron age. Oldest intruding dykes are aged 2.7 Ga. Petrography described in detail.|3.05 +/- 0.25 Ga (Ahmat and de Laeter, 1982).|||Overlain (tectonically or unconformably) by Kantie Murdana Volcanics.|Layered sequence of leucogabbronorite, leucogabbro, leucotroctolite, and olivine gabbronorite cumulates. Broad upward trend from dunite through leucogabbro to ferrogabbro. Rhythmic and cryptic layering are widespread and present on all scales.|
27936|Windimurra Complex|50128|5|Briefly described|p32|Archean|Archean|Age: ca 2800 Ma (Sm-Nd; Ahmat and Ruddock 1990). Geological Province: Yilgarn Craton.||||||07-NOV-08
27936|Windimurra Complex|60460|6|Mentioned|p69|||Shown as Windimurra Mafic Complex on p60 fig 2-75||||||30-APR-15
27936|Windimurra Complex|61144|6|Mentioned|p86 Fig. 26|||Used in a structural context.||||||
27936|Windimurra Complex|64771|5|Briefly described|p7|Neoarchaean|Neoarchaean||2800 Ma (Sm-Nd: Ahmat and Ruddock, 1990).||||Layered mafic-ultramafic intrusions contain significant deposits of vanadiferous magnetite, with potential for Ni, Cu and PGEs.|
83159|Windimurra Intrusive Complex|72494|5|Briefly described|p24-25|||Murchison Domain, Youanmi Terrane, Yilgarn Craton. These dry magmas indicate the Mantle beneath the Murchison Domain was heterogeneously hydrated.|c.2813 Ma.|||||
29154|Windimurra complex|37795|6|Mentioned|p184|||||||||
29154|Windimurra complex|40337|6|Mentioned|p6|||||||||
40355|Windimurra suite|23922|5|Briefly described|p1252|Archean|Archean|Informal-see Windimurra Complex.  Geological Province: Yilgarn Craton.||||||07-NOV-08
79822|Windine Supersuite|69583|5|Briefly described|p49|Mesoarchean|Mesoarchean|Murchison Domain.|||Bunnawarra Suite|||
79822|Windine Supersuite|69584|6|Mentioned|p5 Fig.2|Mesoarchean|Mesoarchean||||Bunnawarra Suite|||
79822|Windine Supersuite|69586|5|Briefly described|p22|Mesoarchean|Mesoarchean|Murchison Domain.|||Bunnawarra Suite.|||
32738|Windjana Gorge reef complex|44998|14|Not recorded|p.51|||||||||
83265|Windmill Hill Quartzite|72259|6|Mentioned|p4|||[Possibly a variation on Windmill Hill quartzite]. Rutile from this unit was used as a reference standard.||||||
29875|Windplain Subgroup|7471|5|Briefly described|p4, Map legend|Proterozoic|Proterozoic|A sag-basin succession.||Unit in Yerrida Group.|Includes Juderina and Johnson Cairn Formations.|Is overlain by Mooloogool Subgroup.|Shallow-water arenite and conglomerate, silicified evaporitic rocks, and stromatolitic carbonate rocks overlain by deeper water siltstones, shales, and carbonate rocks.|
29875|Windplain Subgroup|12099|4|Described|p677-8, 680, 683, Figs.2, 4, 5|Paleoproterozoic|Paleoproterozoic|New or redefined unit by Occhipinti et al. (1997). Unconformably overlies Archean basement. Deposited in a continental fluvial, intertidal to supratidal and shelf environments in a sag basin structure.||Unit in Yerrida Group.|Includes Juderina and Johnson Cairn Formations.|Conformably overlain by Mooloogool Subgroup.|Siliciclastic rocks, stromatolitic carbonates and evaporites.|04-MAR-13
29875|Windplain Subgroup|22501|5|Briefly described|p117|||part of the Yerrida Group||||||
29875|Windplain Subgroup|22694|5|Briefly described|p7|||Yerrida Group||||||
29875|Windplain Subgroup|22716|5|Briefly described|p229|Paleoproterozoic|Paleoproterozoic|Underlies Mooloogool Subgroup.||||||07-NOV-08
29875|Windplain Subgroup|22940|4|Described|Fig.1 p3|||Sag-basin succession. See also Table 2 p12.||||||
29875|Windplain Subgroup|23151|5|Briefly described|p68 Fig.2|||||||||
29875|Windplain Subgroup|23413|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group, Yerrida Basin||||||
29875|Windplain Subgroup|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group,Yerrida Basin||||||07-NOV-08
29875|Windplain Subgroup|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Yerrida Group in the Yerrida Basin||||||07-NOV-08
29875|Windplain Subgroup|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group||||||07-NOV-08
29875|Windplain Subgroup|23589|4|Described|p15|||Of Yerrida Group.||||||
29875|Windplain Subgroup|23593|4|Described|p6|||Of Yerrida Group. Overlying unit Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23597|4|Described|p8|||Of Yerrida Group. Overlying unit Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23600|4|Described|p8|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|23744|5|Briefly described|p2 Fig 1|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|23747|5|Briefly described|p4 table 1|Paleoproterozoic|Paleoproterozoic|See also page 9. Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23749|4|Described|p6|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23759|5|Briefly described|p15|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|23865|5|Briefly described|p169|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|23890|5|Briefly described|p21 Fig.11|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|24021|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin||||||07-NOV-08
29875|Windplain Subgroup|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group.  Geological Province: Yerrida Basin.||||||07-NOV-08
29875|Windplain Subgroup|24535|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Maximum age based on Pb/Pb age of 2173 +/-63 Ma for stromatolitic carbonate at the base of the Windplain Subgroup||Of Yerrida Group.?||||26-NOV-13
29875|Windplain Subgroup|43831|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29875|Windplain Subgroup|43836|5|Briefly described|Map Legend||Proterozoic|||||||
29875|Windplain Subgroup|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Yerrida Group.||||||18-MAY-04
29875|Windplain Subgroup|43843|5|Briefly described|Map Legend||Proterozoic|||||||
29875|Windplain Subgroup|44204|5|Briefly described|Map Legend||Proterozoic|||||||
29875|Windplain Subgroup|44830|5|Briefly described|Map Legend||Proterozoic|||||||
29875|Windplain Subgroup|49893|4|Described|p8|Proterozoic|Proterozoic|Of the Yerrida Group. Geological Province: Yerrida Basin. See also p2 Fig.1.||||||
29875|Windplain Subgroup|49896|5|Briefly described|p4 Fig. 1|||Of the Yerrida Group. Includes the Juderina and Johnson Cairn Formations. ||||||
29875|Windplain Subgroup|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Yerrida Group.  Geological Province: Yerrida Basin.||||||
29875|Windplain Subgroup|50222|5|Briefly described|p321, p333 Tb. 2|Paleoproterozoic|Paleoproterozoic|Superseded by Windplain Group.  Age: <2.2-2.1Ga.||||||07-NOV-08
29875|Windplain Subgroup|61269|5|Briefly described|p86 Fig.1|Paleoproterozoic|Paleoproterozoic|Of the Yerrida Group.||||||07-NOV-08
29875|Windplain Subgroup|61271|5|Briefly described|p104, p105 Fig.1|||Of the Yerrida group. Dominated by siliclastic and evaporitic sediments.||||||
29875|Windplain Subgroup|62289|4|Described|plate 1, p3 Fig. 1, p4, p6-8, p12|Palaeoproterozoic|Palaeoproterozoic|Of Yerrida Group; includes Juderina and overlying Johnson Cairn Formations; is overlain conformably by Mooloogool Subgroup; siliciclastic rocks, evaporites, argillites, and locally turbidites; deposited in supratidal and intertidal environments (shallow and lower energy setting); Sedimentological characteristics indicative of a sag basin or pre-rift depression; shallower lower energy setting compared with overlying Mooloogool Subgroup.||||||
29875|Windplain Subgroup|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.|||Includes Johnson Cairn and Juderina Formations.|||14-APR-11
29875|Windplain Subgroup|63866|5|Briefly described|p165|||Yerrida Basin.||Yerrida Group|Includes the Juderina Formation and the Johnson Cairn Formation.|Conformably overlain by the Mooloogool Subgroup.||
29875|Windplain Subgroup|64724|5|Briefly described|p43|Rhyacian|Rhyacian|Pb-Pb isochron age of 2173 +/- 64 Ma from stromatolitic carbonates.||||||02-APR-12
29875|Windplain Subgroup|65264|5|Briefly described|p26|||Of the Yerrida Group. Includes the Juderina Formation. Unconformably overlain by Mooloogool Subgroup. Geological province: Yerrida Basin.||||||07-FEB-11
29875|Windplain Subgroup|65408|5|Briefly described|pp82-83, p84 Fig.1, p85|Paleoproterozoic|Rhyacian|A sag-basin succession deposited in a predominantly shallow-water to evaporitic environment.|Deposited c.2.2 Ga.|Lower unit in Yerrida Group.|Comprises Juderina and Johnson Cairn Formations.|Locally transitionally overlain by Mooloogool Subgroup.||
29875|Windplain Subgroup|65411|6|Mentioned|p89 Fig.1.|||||Lower unit in Yerrida Group.||||
29875|Windplain Subgroup|65412|5|Briefly described|p97 Fig.1, p99.|Paleoproterozoic|Paleoproterozoic|Interpreted to represent an early sag basin.||Unit in Yerrida Group.|||Siliciclastics, evaporites, stromatolitic carbonate rocks, shales.|
29875|Windplain Subgroup|65419|2|Defined|p4 Fig.1, pp7-8, p10 Fig.3, p19.|Paleoproterozoic|Paleoproterozoic|Named after Windplain Bore. Type area: Glengarry and central Peak Hill 1:250 000 sheets. Variable thickness to 2000 m.|2.2 Ga (Russel et al. 1994).|Lower unit in Yerrida Group.|Includes Juderina and Johnson Cairn Formations.|Is faulted against Bryah Group. Is conformably overlain by Mooloogool Subgroup.|Terrigenous clastic rock, carbonate, evaporite and minor wacke.|
29875|Windplain Subgroup|65913|5|Briefly described|p2 Fig.1, p5.|Paleoproterozoic|Paleoproterozoic|A sag-basin succession.||Unit in Yerrida Group.|Includes Juderina and Johnson Cairn Formations.|||24-MAY-16
29875|Windplain Subgroup|66427|6|Mentioned|p40 Fig.1|||||Unit in Yerrida Group.|||Evaporites and siliciclastics.|
29875|Windplain Subgroup|68561|5|Briefly described|GLENGARY_GEOLOGYP_LUT.csv||Proterozoic|Yerrida Basin. [replaced by Windplain Group]||Yerrida Group||||
29875|Windplain Subgroup|70796|5|Briefly described|glengarry_100k_geologyp_lut.csv|||Yerrida Basin. Misspelt? See also Windplain Group. Also appears in Glengarry100_2645_stratig.pdf.||Yerrida Group||Includes the Johnson Cairn Formation and the Juderina Formation.||
29875|Windplain Subgroup|70804|5|Briefly described|p2, p37, p45|||Forms the eastern part of the former 'Glengarry Basin'. Developed in a sag basin.||Yerrida Group|Includes the Johnson Cairn Formation and Juderina Formation.|||
29875|Windplain Subgroup|71484|5|Briefly described|p122,124|||. Abandoned, see Windplain Group (Pirajno et al., 2004).||Unit of Yerrida Group.||||30-AUG-19
30211|Wingelina Complex|23745|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Also called Musgrave Complex. Age: c.1550-1200 Ma.||||||
30211|Wingelina Complex|43118|6|Mentioned|p28|||[Probably misspelt. variation  place name Wingelinna?||||||13-FEB-09
30211|Wingelina Complex|43348|6|Mentioned|P15|||||||||
30211|Wingelina Complex|43442|6|Mentioned|p17,20,34|||May be a geological province rather than stratigraphic name.||||||
30211|Wingelina Complex|44139|6|Mentioned|p275, p283-4, p285 Fig. 3-69|||Province-level unit? Southeastern Paterson Orogen: formerly referred to as Musgrave Block. Gravity data suggests subsurface link with Rudall Complex. Comprising the Musgrave-Mann and Giles Complexes, and the Olia Gneiss. High grade metamorphic and plutonic rocks.| | ||||06-MAR-18
30211|Wingelina Complex|65102|6|Mentioned|p368, 373|||Older than Punkerri & Wirrildar Formations.||||||
30211|Wingelina Complex|67856|6|Mentioned|p335, p337|||Highly deformed basement under Amadeus Basin.||||Overlain by Dean Quartzite (unconformably).||
70176|Wingellina Hills gabbro/pyroxenite intrusion|44109|4|Described|p10, p48-49|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Olivine gabbro and gabbronorite, containing lenticular stratabound intercalations of pyroxenite and peridotite. Max. thickness: 1600m. ||||||
79623|Wingellina Hills intrusion|68996|6|Mentioned|p47, 50, 57, 59, 62, 64|Mesoproterozoic|Mesoproterozoic|Part of G1 group. Described as 'connected to Hinckley intrusion'. ||Giles Suite.||||
69761|Wingellina gabbro/pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: >1600m.||||||21-SEP-05
78326|Wingellina intrusion|65135|6|Mentioned|p14|||Informal name. Peridotitic. Of the Giles layered mafic-ultramafic intrusions.||||||16-JAN-15
29155|Winifred formation|41215|6|Mentioned|p280|||||||||
29155|Winifred formation|69693|6|Mentioned|p2, 4, 6|||Lennard Shelf, Canning Basin.||Grant Group||||
81290|Winnamea Sandstone|69547|5|Briefly described|p182,192-193,197|Artinskian|Artinskian|Southern Carnarvon Basin. Also referred to as Winnamea Sandstone Member on p193, Winnemea Sandstone p192, Winnemea Sandstone Member p193, 197. Glacially-influenced succession, and correlable with Ballythanna Sandstone and High Cliff Sandstone.||Unit of Callytharra Formation.||||24-AUG-20
82119|Winnamea Sandstone Member|72910|5|Briefly described|p4|Sakmarian|Sakmarian|Shown as being recognised in Merlinleigh Sub-basin, Carnarvon Basin. [Misspelling of Winnemia Sst Mbr?]||Callytharra Formation||||
82120|Winnemea Sandstone Member|72910|6|Mentioned|p15|||Jimba Syncline. [Misspelling of Winnemia Sst Mbr?]||||||
68860|Winnemia Sandstone|60331|6|Mentioned|p33|||||||||
68860|Winnemia Sandstone|67977|6|Mentioned|p491|||Shortening of Winnemia Sandstone Member in text. See Winnemia Sandstone Member.||||||18-SEP-14
29156|Winnifred Formation|46912|6|Mentioned|p131|||Refs Crowe & others(1978). Misspeling of res.name Winifred Formation.||||||
69370|Winning Group shales|60118|6|Mentioned|p29|||Informal reference to shales in the Winning Group (i.e. Muderong Shale and Gearle Siltstone). Geological Province: Barrow Sub-basin, North Carnarvon Basin.||||||14-NOV-07
73767|Winning Group, Lower|24351|6|Mentioned|p24|||Informal - see Winning Group. Geological Province: Exmouth Sub-basin.||||||13-DEC-07
77195|Winning Sandstone Member|61811|6|Mentioned|p8. |Cretaceous|Cretaceous|Misspelling of  Windalia Sandstone Member? see p9.||Unit in Muderong Shale.||||10-SEP-12
77195|Winning Sandstone Member|64635|5|Briefly described|p7 |||Said to be of the Muderong Shale [cf. same claim in RefID 61811].||||||
32908|Winning Series|48861|14|Not recorded|p.5|||Ref. Raggatt, 1936.||||||
70700|Wirrildar beds''|62453|6|Mentioned|p50|||Overlies: Punkerri Sandstone.||||||
33916|Withorpe Formation|22493|5|Briefly described|p96 Fig.6|||||||||
73996|Wittecarra Sandstone Member|14227|5|Briefly described|p7, p10|Triassic|Triassic|Basal sands of Kockatea Shale. See also Enclosure 2.||||||07-FEB-11
29160|Wittecarra Sandstone""|41271|6|Mentioned|p116|||||||||
80029|Wittecarra Sequence|69297|6|Mentioned|p207|Triassic|Permian|Play type previously variously referred to as Dongara, Wagina or Wittecarra sequences. Sealed by Kockatea Sequence||||||20-SEP-17
26226|Wittenoom Dolomite|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
26226|Wittenoom Dolomite|23746|6|Mentioned|p21|||Renamed Wittenoom Formation.||||||
26226|Wittenoom Dolomite|24025|5|Briefly described|p14|Archean|Archean|Age: 2560+/-5Ma (SHRIMP zircon).  Geological Province: Hamersley Basin.||||||07-NOV-08
26226|Wittenoom Dolomite|24041|5|Briefly described|p493|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
26226|Wittenoom Dolomite|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Hamersley Group. Overlain by Mount Sylvia Formation. Overlies Marra Mamba Iron Formation. Geological Province: Hamersley Province.||||||07-FEB-11
26226|Wittenoom Dolomite|29596|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|29716|4|Described|Table 1|||||||||
26226|Wittenoom Dolomite|29717|6|Mentioned|p1157|||||||||
26226|Wittenoom Dolomite|30685|6|Mentioned|p907|||||||||
26226|Wittenoom Dolomite|31671|5|Briefly described|p11|||||||||
26226|Wittenoom Dolomite|32326|6|Mentioned|p122|||Hamersley Gp.||||||
26226|Wittenoom Dolomite|33538|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|33540|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|33542|6|Mentioned|p412|||||||||
26226|Wittenoom Dolomite|33544|2|Defined|p85|Proterozoic|Proterozoic|||||||
26226|Wittenoom Dolomite|33687|5|Briefly described|p917|||||||||
26226|Wittenoom Dolomite|34066|4|Described|p5|||L.Prot.||||||
26226|Wittenoom Dolomite|34128|6|Mentioned|p17|||See also P18||||||
26226|Wittenoom Dolomite|34129|5|Briefly described|p57|||See also P58||||||
26226|Wittenoom Dolomite|34135|5|Briefly described|Table 1|||See also Table 2, PP6,7,11-13. Lower Proterozoic||||||
26226|Wittenoom Dolomite|34471|6|Mentioned|p22|||||||||
26226|Wittenoom Dolomite|34999|6|Mentioned|Table 17|||||||||
26226|Wittenoom Dolomite|35052|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|35059|6|Mentioned|Table.19|||||||||
26226|Wittenoom Dolomite|35260|5|Briefly described|p14|||||||||
26226|Wittenoom Dolomite|35299|5|Briefly described|p893|||||||||
26226|Wittenoom Dolomite|35976|6|Mentioned|Fig.39|||||||||
26226|Wittenoom Dolomite|36091|6|Mentioned|p572|||||||||
26226|Wittenoom Dolomite|36247|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|36268|6|Mentioned|p176|||Aquifer.||||||12-MAR-08
26226|Wittenoom Dolomite|36551|6|Mentioned|Table 23|||||||||
26226|Wittenoom Dolomite|36642|6|Mentioned|Table 1|||||||||
26226|Wittenoom Dolomite|36882|4|Described|p134|||||||||
26226|Wittenoom Dolomite|37170|6|Mentioned|p200|||||||||
26226|Wittenoom Dolomite|37297|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|37460|6|Mentioned|Fig.3.4|||||||||
26226|Wittenoom Dolomite|37704|6|Mentioned|p507|||||||||
26226|Wittenoom Dolomite|37708|6|Mentioned|p1930|||||||||
26226|Wittenoom Dolomite|38776|5|Briefly described|Table 1|||||||||
26226|Wittenoom Dolomite|38790|6|Mentioned|Table 1|||||||||
26226|Wittenoom Dolomite|38988|6|Mentioned|p6|||||||||
26226|Wittenoom Dolomite|39200|4|Described|p285|||||||||
26226|Wittenoom Dolomite|39210|5|Briefly described|Table 1|||||||||
26226|Wittenoom Dolomite|39558|6|Mentioned|Table 1|||||||||
26226|Wittenoom Dolomite|39697|6|Mentioned|p15|||See also P125||||||
26226|Wittenoom Dolomite|40369|6|Mentioned|Plate 1|||||||||
26226|Wittenoom Dolomite|40987|6|Mentioned|p16|||||||||
26226|Wittenoom Dolomite|41358|6|Mentioned|Fig.2|||||||||
26226|Wittenoom Dolomite|41622|5|Briefly described|p269|||See also Fig.4||||||
26226|Wittenoom Dolomite|41669|6|Mentioned|p28|||||||||
26226|Wittenoom Dolomite|41768|5|Briefly described|Table 1|||See also P27||||||
26226|Wittenoom Dolomite|42013|5|Briefly described|Map legend|Archean||||||||07-NOV-08
26226|Wittenoom Dolomite|42112|4|Described|p8|||||||||
26226|Wittenoom Dolomite|42148|6|Mentioned|Table 1 P687|||||||||
26226|Wittenoom Dolomite|42190|6|Mentioned|p274-5 Fig.4 map|||||||||
26226|Wittenoom Dolomite|42352|6|Mentioned|p22|||||||||
26226|Wittenoom Dolomite|42471|4|Described|p7|||||||||
26226|Wittenoom Dolomite|42472|5|Briefly described|Map legend|||||||||
26226|Wittenoom Dolomite|42495|5|Briefly described|p35|||||||||
26226|Wittenoom Dolomite|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
26226|Wittenoom Dolomite|42704|5|Briefly described|Plate 2E||Archean|Of the Hamersely Group. Combined with Mount McRae Shale and Mount Sylvia Formation in this map legend.||||||07-NOV-08
26226|Wittenoom Dolomite|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
26226|Wittenoom Dolomite|42744|4|Described|p4|||||||||
26226|Wittenoom Dolomite|42898|5|Briefly described|Fig.2 P341|||of Hamersley Group||||||
26226|Wittenoom Dolomite|43055|6|Mentioned|p17|||||||||
26226|Wittenoom Dolomite|43063|5|Briefly described|p49|||||||||
26226|Wittenoom Dolomite|43064|5|Briefly described|p67|||Superseded by Wittenoom Formation||||||
26226|Wittenoom Dolomite|43119|5|Briefly described|p9|||of Hamersley Group||||||
26226|Wittenoom Dolomite|43210|5|Briefly described|Table 1 p3,p4.||Archean|of Hamersley Group.||||||07-NOV-08
26226|Wittenoom Dolomite|43290|6|Mentioned|p6||Archean|of Hamersley Group. Superceded by Wittenoom Formation.||||||07-NOV-08
26226|Wittenoom Dolomite|43595|6|Mentioned|Fig.2-49,p220|||||||||
26226|Wittenoom Dolomite|44152|5|Briefly described|p178-180|||The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Hamersley Group||Overlies Marra Mamba Iron Formation. Equivalent to Carawine Dolomite. Is overlain by Mount Sylvia Formation.|Limestone, dolomite, chert, argillite, tuff.|
26226|Wittenoom Dolomite|44438|14|Not recorded|map legend||Paleoproterozoic|Formation of Hamersley Group of Mt. Bruce Supergroup. L.Proterozoic.||||||07-NOV-08
26226|Wittenoom Dolomite|44477|4|Described|p.10, Table 1||Proterozoic|SF/50-6.||||||
26226|Wittenoom Dolomite|44478|14|Not recorded|map legend||Proterozoic|||||||
26226|Wittenoom Dolomite|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
26226|Wittenoom Dolomite|44501|4|Described|p.7,17,tb.4,7, map||Paleoproterozoic|(ref. to MacLeod et al 1963). (F/50-7). See also p.18,19,21,30, for more details. Lower Proterozoic.||||||07-NOV-08
26226|Wittenoom Dolomite|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26226|Wittenoom Dolomite|44503|2|Defined|p.6,7,8,Tb.2, map|||Roy Hill Sheet. (F50-12). See also p.13,14,17-19, for more details.||||||
26226|Wittenoom Dolomite|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26226|Wittenoom Dolomite|44692|4|Described|p.7,11-13,15,21,Tb.1|||(F50-11).||||||
26226|Wittenoom Dolomite|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
26226|Wittenoom Dolomite|46899|6|Mentioned|p8|||Heat flow||||||
26226|Wittenoom Dolomite|50224|6|Mentioned|p380 Fig. 6|||Geological Province: Hamersley Province.||||||07-FEB-11
26226|Wittenoom Dolomite|50227|5|Briefly described|p443 Fig. 1|Archean|Archean|Of the Hamersley Group.  Age: 2561Ma.  Geological Province: Hamersley Province.||||||07-FEB-11
26226|Wittenoom Dolomite|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
26226|Wittenoom Dolomite|62021|5|Briefly described|p169|Proterozoic|Proterozoic|Karstified and contains cavernous zones.||||||
26226|Wittenoom Dolomite|62129|6|Mentioned|p9, p20|Archaean|Archaean|Superseeded name, now Wittenoom Dolomite.||||||07-FEB-11
26226|Wittenoom Dolomite|63153|6|Mentioned|p1370. |||See Wittenoom Formation (p1359-1360, p1361 Fig.2, p1363, p1368).||||||
26226|Wittenoom Dolomite|64384|5|Briefly described|p35 Tb. 6, p36|||Of Hamersley Gp. Its basal shale now named West Angelas Shale. Overlies Mount Newman Member (Marra Mamba Fm). Geol.prov: Hamersley Basin.Comprises massive crystalline dolomite, passing up into interbedded thin shales, cherts, dolomites + occasional BIF||||||07-FEB-11
26226|Wittenoom Dolomite|64725|6|Mentioned|p58.|||||Unit in Hamersley Group.||Overlies Marra Mamba Iron-formation. Is overlain by Mount Silvia Formation.||
26226|Wittenoom Dolomite|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
26226|Wittenoom Dolomite|65194|6|Mentioned|p15 Fig.2.3, p16 Fig.2.4, p96, p99-101|Early Proterozoic|Early Proterozoic|Dolomite and shale. Underlies Millstream Dolomite. Erosion of this unit by Fortescue River and precursors formed the WNW-trending Fortescue Plain.||||||
26226|Wittenoom Dolomite|65683|6|Mentioned|p799|||See Wittenoom Formation.||||||08-MAR-12
26226|Wittenoom Dolomite|65829|6|Mentioned|p24.|||See Wittenoom Formation. 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.||||||
26226|Wittenoom Dolomite|67025|4|Described|pp318-320, pp322-326, p328.|||||Unit in Hamersley Group.||Conformably overlies Marra Mamba Iron Formation. Is overlain conformably by Mount Sylvia Formation.||
26226|Wittenoom Dolomite|67130|6|Mentioned|p8 fig 5, p39 fig 36, p51|||Outdated name, replaced by Wittenoom Formation||||||
26226|Wittenoom Dolomite|67183|6|Mentioned|p643|||Neoarchean? Name superseded by Wittenoom Formation )see p645 Tb.1).||||Apparent lateral equivalent to the Carawine Dolomite.||
26226|Wittenoom Dolomite|67855|6|Mentioned|p226|||||||||
26226|Wittenoom Dolomite|69754|6|Mentioned|p331|||Pilbara Craton.||Hamersley Group||||
26226|Wittenoom Dolomite|70509|5|Briefly described|p14,28|Neoarchean|Neoarchean|Geological province: Hamersley Province; Pilbara Craton. Also referred to as Wittenoom Formation on p28.||Unit of Hamersley Group.||Overlain by Mount McRae Shale. Underlain by Marra Mamba Iron Formation.||
26226|Wittenoom Dolomite|70826|6|Mentioned|p8|Neoarchean||||||Overlain by the Pinjian Chert Breccia.||
26226|Wittenoom Dolomite|72758|5|Briefly described|p15-16 Tb.1, p23-24.|||This unit is 150 m thick on the southern limb of the Jeerinah Anticline. Informally subdivided into 2.||Hamersley Group||Conformably overlies Marra Mamba Iron Formation and conformably underlies Mount Sylvia Formation.|Thin to medium-bedded dolomite with mudstone, chert, and minor BIF. Dolomites may contain slump structures.|
35658|Wittenoom Dolomite Formation|23126|4|Described|p382|||||||||
70371|Wittenoom Formation, upper|61577|5|Briefly described|p786 Tb. 1|Archean|Archean|Informal name. Geological Province: Hamersley Basin.||||||07-NOV-08
70211|Wittenoom arenite|61576|6|Mentioned|p774|||||||||
70208|Wittenoom spherule layer|61575|3|Fully described|p760, p761|Neoarchean|Neoarchean|Informal -spherule layer within the Bee Gorge Member of the Wittenoom Formation; interpreted as impact-generated melt. Age: 2541+18/-15Ma. Geol. Prov: Hamersley Basin.||||||07-NOV-08
70208|Wittenoom spherule layer|61576|4|Described|p774 Fig. 1|Neoarchean|Neoarchean|Informal name - refers to impact spherule layer within the Wittenoom Formation. Age: 2541+18/-15Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
78752|Woddiana Sandstone Member|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean|[Mis-spelling of Woodiana].||Unit in Jeerinah Formation.||Is overlain by Roy Hill Shale Member.||
39777|Wodgina Main Lode Pegmatite|24193|4|Described|p885, p886 Tb.5|Archean|Archean|Of the Wodgina pegmatite group. Not intended as a formal name. See also Wodinga main lode pegmatite. Geological Province: Pilbara Craton.||||||07-NOV-08
39778|Wodgina main lode pegmatite|24193|4|Described|p883-885, p886 Tb.5|Archean|Archean|Of the Wodgina pegmatite group. Geological Province: Pilbara Craton. See also Wodgina Main Lode Pegmatite.||||||07-NOV-08
73787|Wodgina main-lode pegmatite|50542|6|Mentioned|p108, p111|Archean|Archean|Informal name. Thickness: 40m.||||||07-FEB-11
38606|Wodgina pegmatite group|23784|4|Described|p46|Archean|Archean|Informal. Not a stratigraphic name.||||||07-NOV-08
38606|Wodgina pegmatite group|24193|4|Described|p883|Archean|Archean|Includes the Wodgina main lode pegmatite. Geological Province: Pilbara Craton.||||||07-NOV-08
37061|Wogalli Sandstone|23726|5|Briefly described|p8 Fig 2c|Early Cretaceous|Early Cretaceous|Overlying unit Birdrong Sandstone. Geological Province: Carnarvon Basin.||||||
37061|Wogalli Sandstone|67200|5|Briefly described|p8 fig 6, |Cretaceous|Cretaceous|||||Unconformably overlain by Birdrong Sandstone|Crudely and trough cross bedded sandstone.|
27658|Wollubar Sandstone|22769|5|Briefly described|Table1p759||Middle Eocene|||||||
27658|Wollubar Sandstone|23797|5|Briefly described|p3|Late Eocene|Middle Eocene|Underlies Perkolilli Shale (conformable). Geological Province: Yilgarn Craton.||||||
27658|Wollubar Sandstone|23989|5|Briefly described|p51|Middle Eocene|Middle Eocene|See also page 52. Geological Province: Yilgarn Craton||||||
27658|Wollubar Sandstone|24160|6|Mentioned|p117.|||||||Is overlain conformably by Perkolilli Shale.||
27658|Wollubar Sandstone|24397|5|Briefly described|p236|||Now included in North Royal Formation and Werillup Formation.  Geological Province: Eucla Basin.||||||
27658|Wollubar Sandstone|42535|3|Fully described|p16|late Eocene|middle Eocene|Name reserved. Age: late Middle to early Late Eocene.||||||
27658|Wollubar Sandstone|43065|2|Defined|p88|Late Eocene|Middle Eocene|||||||
27658|Wollubar Sandstone|43279|6|Mentioned|Map Legend||Tertiary|||||||
27658|Wollubar Sandstone|43280|6|Mentioned|Map Legend||Tertiary|||||||
27658|Wollubar Sandstone|43623|5|Briefly described|p4|Late Eocene|Middle Eocene|||||||
27658|Wollubar Sandstone|43838|5|Briefly described|p4, 8, 9||Tertiary|Occurs in Roe Palaeodrainage.||||||12-JUL-16
27658|Wollubar Sandstone|61197|5|Briefly described|p473, p474 Fig.2, p478-479|Middle Eocene|Middle Eocene|A basal, coarse-grained fluviatile unit in-filling inset-valleys cut into Permian tunnel valleys which in turn are incised into Precambrian basement.||||Is overlain unconformably by Perkolilli Shale.|Sand, clay, conglomerate.|
27658|Wollubar Sandstone|61814|5|Briefly described|p23|Tertiary|Tertiary|Consists of sand, ferruginous gravel and fragments of ferruginous duricrust.||||||08-FEB-10
27658|Wollubar Sandstone|65194|5|Briefly described|p139-149, p153 Fig.4.46, p157 Fig.4.50|Late Eocene|Middle Eocene|(Commander et al. 1992). Basal unit in Roe Palaeovalley. Unconformably underlies the Perkolilli Shale. Maximum thickness of 38m. Quartz-dominated sediments: unlithified fine- to very coarse-grained sand, deposited mostly in a fluvial environment. Correlated with the Hampton Sandstone in the Lefroy Palaeovalley.  The principal aquifer in the eastern Yilgarn.||||||08-APR-16
27658|Wollubar Sandstone|65204|6|Mentioned|p22|Late Eocene|Middle Eocene|Quartz sand with subordinate conglomerate, clay, carbonaceous silt and lignite.||||||
27658|Wollubar Sandstone|65262|5|Briefly described|p4-14|Eocene|Eocene|Yilgarn Craton. Up to 28m thick. Late Middle to early Late Eocene in age. Highly permeable and contains significant volumes of groundwater; is the largest source on KALGOORLIE. Confined by Perkolilli Shale and its equivalents.||||Overlain by the Perkolilli Shale.|Unconsolidated quartz sand, with minor conglomerate, silt, clay and lignite.|
79184|Wongarra Rhyolite|65757|6|Mentioned|p84 Fig.2, p88 Fig.8|||Underlies the Boolgeeda Formation, overlies the Weeli Weeli Formation. ||||||
25644|Wongarra Volcanics|23126|5|Briefly described|p383 Fig.3|||||||||
25644|Wongarra Volcanics|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Hamersley group.  Age: c.2.74Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
25644|Wongarra Volcanics|31828|6|Mentioned|p40|||Stratigraphic table||||||
25644|Wongarra Volcanics|33544|6|Mentioned|p34|||Misspelling of Woongarra||||||
25644|Wongarra Volcanics|35218|6|Mentioned|Fig.1|||||||||
25644|Wongarra Volcanics|37327|6|Mentioned|p389|||||||||
25644|Wongarra Volcanics|67025|6|Mentioned|p324 Table 8.|||Typo for Woongarra Volcanics (pp318-320, p322 Table 3, p324 Table 8.)||||||24-APR-12
25644|Wongarra Volcanics|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Hamersley Group||||
25644|Wongarra Volcanics|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|Oakover Basin.||Hamersley Group||||
40068|Wongarra volcanics|23936|4|Described|Tb.1|Paleoproterozoic|Archean|Age: c.2.47 Ga. Geological Province: Pilbara Craton. Overlying Unit: Boolgeeda Iron Formation. Underlying Unit: Weeli Wolli Iron Formation. Parent: Hamersley Group.||||||07-NOV-08
41221|Wongawol formation|50223|6|Mentioned|p346|||Informal - see Wongawol Formation.||||||
41091|Wongi basalt|24139|5|Briefly described|p239 Table 1|||Geological Province: Ora Banda Domain.  Of the Pole Group.||||||
37102|Wonyugunna Sandstone|23747|5|Briefly described|p16|Proterozoic|Proterozoic|Of Bangemall Group. Geological Province: Bangemall Basin.||||||
39889|Woodbruck Formation|23784|5|Briefly described|p10|||Of Whundo Group||||||
73596|Woodiana stromatolite|62579|6|Mentioned|p122|Archean|Archean|Informal reference to the stromatolite occurrences in Woodiana Member of the Jeerinah Formation. Age: 2.7Ga. Geological Province: Pilbara Craton.||||||22-OCT-15
37087|Woodlands Arenite|23723|6|Mentioned|p95|||See Woodlands Arenite Member.||||||
37087|Woodlands Arenite|64287|5|Briefly described|p34 Fig. 2|||Should probably be Woodlands Arenite Member - of Gap Well Formation. Coarse-grained sandstone.  Geological province: Jillawarra Sub-basin.||||||07-FEB-11
27013|Woodline Beds|29681|6|Mentioned|p191|||||||||
27013|Woodline Beds|29784|6|Mentioned|Fig.16|||||||||
27013|Woodline Beds|30012|6|Mentioned|p12|||||||||
27013|Woodline Beds|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
27013|Woodline Beds|30883|6|Mentioned|Fig. 2|||||||||
27013|Woodline Beds|30974|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27013|Woodline Beds|31393|6|Mentioned|Pl.25|||||||||
27013|Woodline Beds|33573|6|Mentioned|Fig.1|||||||||
27013|Woodline Beds|33595|6|Mentioned|p19|||||||||
27013|Woodline Beds|36551|6|Mentioned|p141|||||||||
27013|Woodline Beds|36872|3|Fully described|p79|||||||||
27013|Woodline Beds|36876|6|Mentioned|p101|||||||||
27013|Woodline Beds|37299|6|Mentioned|p88|||||||||
27013|Woodline Beds|37460|4|Described|p179|||||||||
27013|Woodline Beds|38764|6|Mentioned|p112|||||||||
27013|Woodline Beds|41635|4|Described|p19|||||||||
27013|Woodline Beds|41771|4|Described|p45|||||||||
27013|Woodline Beds|42724|5|Briefly described|map legend|Proterozoic||||||||
27013|Woodline Beds|46316|2|Defined|p.12,13||Neoproterozoic|Map, p.5, Tb.1, opposite p.6,9,15. (H51-14).?Upper Prot.||||||
27013|Woodline Beds|60076|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Geological Province: Yilgarn Craton.||||||07-NOV-08
27013|Woodline Beds|64161|5|Briefly described|p583-584|||Obsolete name for Woodline Formation given by Sofoulis and Bock (1962). Described by Sofoulis and Brock (1962) as shallow water sediments of Upper Proterozoic age.||||||21-MAR-12
27013|Woodline Beds|64340|6|Mentioned|p23-24|||Superseded and replaced by Woodline Formation. Named by Sofoulis and Bock (1963).||||||21-MAR-12
27013|Woodline Beds|65260|6|Mentioned|p14|||Now known as Woodline Formation||||||
29169|Woodline beds|24160|6|Mentioned|p150.|||Northern foreland of Albany-Fraser Orogen.||||||
29169|Woodline beds|41771|4|Described|p45|||||||||
29169|Woodline beds|42817|4|Described|p26|||age of 1620 +/- 100 Ma.||||||
29169|Woodline beds|43280|5|Briefly described|Map Legend||Proterozoic|||||||
29169|Woodline beds|43838|5|Briefly described|p3, Fig2 p6, 8||Proterozoic|>250 m thick||||||12-JUL-16
29169|Woodline beds|44137|5|Briefly described|p255, p257 fig 3-43, p259|||Griffin (1998). About 200m thick. Gently folded.|1620 +/- 100 Ma (Rb-Sr isochron; Turek 1966).| Of Mount Barren Group.|||Quartzite and minor phyllite.|30-APR-15
27624|Woodrarrung Formation|23569|4|Described|p4 Tb. 1|Proterozoic|Proterozoic|Formerly Woodrarrung Sandstone.   Parent: Badgeradda Group.   Thin-bedded feldspathic and quartzose sandstone||||||
27624|Woodrarrung Formation|24114|5|Briefly described|p8|Neoproterozoic|Mesoproterozoic|Of Badgeradda Group. Geological Province: Yilgarn Craton.||||||
27624|Woodrarrung Formation|29690|6|Mentioned|p12|||||||||
27624|Woodrarrung Formation|40339|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27624|Woodrarrung Formation|43835|5|Briefly described|Map Legend||Proterozoic|||||||
27624|Woodrarrung Formation|48823|5|Briefly described|p3 Tb. 1|Mesoproterozoic|Paleoproterozoic|Probably misspelt and should be Woodrarrung Sandstone. Of the Badgeradda Group. Thickness: ~1600ft.||||||07-NOV-08
27624|Woodrarrung Formation|64580|4|Described|map legend||Mesoproterozoic|Of Badgeradda Group. Medium- to coarse-grained quartzose sandstone, commonly silicified, overlain by fine- to medium-grained feldspathic sandstone.||||||09-DEC-08
25648|Woodstock Adamellite|39444|2|Defined|Table 3|Archean|Archean|See also Table 2||||||07-NOV-08
25648|Woodstock Adamellite|39697|3|Fully described|p39|||||||||
25648|Woodstock Adamellite|44150|5|Briefly described|p144 Tb.2-21, p149 Fig.2-137|||260 sq. km.||Yule Granitoid Complex||Intrudes Abydos Adamellite and Warrawoona Group greenstones.|Foliated, porphyritic biotite monzogranite.|
25648|Woodstock Adamellite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Superseded by Woodstock Monzogranite. Geological province: Pilbara Craton.||||||07-FEB-11
29994|Woolaga Member|43067|5|Briefly described|p119|||of Holmwood Shale. Misspelling/abbreviation of Woolaga Limestone Member?||||||
39230|Woolgangie Super Suite|23904|6|Mentioned|p49|||Informal- See Woolgangie Supersuite.  Geological Province: Yilgarn Craton.||||||
39231|Woolgangie Supersuite granitoids|23904|5|Briefly described|p29|||Informal name.  Geological Province: Yilgarn Craton.||||||
39232|Woolganie Super Suite|23904|6|Mentioned|p64|||Misspelt - see Woolgangie Supersuite.||||||
29171|Woolganyer Group|34324|6|Mentioned|Table|||||||||
81331|Woolgara Andesite|70030|5|Briefly described|p192|Neoarchean|Neoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Greensleeves Formation.||||
75176|Woolgra Andesite|64891|5|Briefly described|p37 Fig. 2, p40, p48-9 Tb. 1|Archean|Archean|Abbreviated version of Woolgra Andesite Mbr. Of Greensleeves Formation. Over Stockyard Basalt Mbr. Age: 2755+/-5Ma (for feldspar-phyric-andesite). Geological province: Murchison Domain. Andesitic volcanic and volcaniclastic rocks; weakly metamorphosed.||||||07-FEB-11
75176|Woolgra Andesite|71168|6|Mentioned|p25|||||||||
24121|Woolgra Formation|42533|4|Described|p58, p61|||Name reserved.||||||
24121|Woolgra Formation|44149|5|Briefly described|p35 fig 2-30, p38-39, p48 Fig.2-53|Archean|Archean|Of Murchison Province||Porlell Subgroup||Overlies Stockyard Basalt.|Basal 350m of fine- to medium-grained volcanogenic sediments, with andesitic and dacitic volcanic rocks including lava, tuff, breccia and lahar deposits.|
24121|Woolgra Formation|65268|6|Mentioned|p6 fig 4|||||Porlell Subgroup|||Felsic volcaniclastic rocks; minor felsic volcanic rocks.|
37803|Woollaston Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Probably misspelt - see also Woolaston Formation. Geological Province: Vulcan Sub-Basin||||||01-MAR-10
24122|Woolnough Beds|38243|6|Mentioned|Fig.2|||||||||
24122|Woolnough Beds|38898|6|Mentioned|Table 1|||||||||
24122|Woolnough Beds|38988|6|Mentioned|p18|||||||||
24122|Woolnough Beds|45149|2|Defined|p31|Early Cambrian|Early Cambrian|See also Table 1.||||||
24122|Woolnough Beds|46975|6|Mentioned|Fig.3|||||||||
70701|Woolnough Beds''|62453|6|Mentioned|p24|||Informal name.||||||
70704|Woolnough Formation''|62453|6|Mentioned|p18|||Informal name.||||||
70702|Woolnough beds''|62453|6|Mentioned|p24|||Informal name.||||||
70703|Woolnough'' Formation|62453|6|Mentioned|p18|||Informal name.||||||
41240|Wooly dolomite|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Of the lower part of the Wyloo Group.||||||07-NOV-08
77737|Woolyeener Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Norseman Terrane.  Kambalda Sequence.|||||Komatiite, tholeiitic and high MgO basalts.|
77737|Woolyeener Formation|73391|6|Mentioned|Appendices.|||||||Equivalent to Lunnon Basalt.||
83393|Woolyeener Group|73391|6|Mentioned|Appendices. A2 Table 3.1|||Hall and Becker (1965). Regional stratigraphic correlation chart of other workers.|||||Tholeiitic pillow lavas, slate, minor high-Mg basalt.|02-JUL-22
81383|Woolyeenyer Basalt|70326|6|Mentioned|p365|Neoarchean|Neoarchean|Geological province: Norseman Domain, Kalgoorlie Terrane, Yilgarn Craton. See Woolyeenyer Formation p360.||||||15-AUG-19
29261|Woolyeenyer Group|29784|6|Mentioned|Table 1|||||||||
29261|Woolyeenyer Group|30562|4|Described|p37|||Refers Hall & Bekker (1965)||||||
29261|Woolyeenyer Group|30900|5|Briefly described|p67|||See also Table 1||||||
29261|Woolyeenyer Group|33917|5|Briefly described|p178|||||||||
29261|Woolyeenyer Group|37373|5|Briefly described|Table 2.I|||||||||
29261|Woolyeenyer Group|41066|5|Briefly described|2 of 2 C04|||||||||
29261|Woolyeenyer Group|45543|4|Described|p.102||Archean|Contains (top to bottom): Desirable Pillow Lava, Crown Basalt, Nulsen Slate, Royal Amphibolite, Bluebird Gabbro, Gee Cee Slate, Mararoa Pillow Lava, Venture Slate, Kingswood Basalt.||||||07-NOV-08
77462|Woomarel Group|67370|6|Mentioned|p327.|Artinskian|Artinskian|Carnarvon Basin. Alpine glacial episodes.||||||
82279|Woomerangee member""|69558|6|Mentioned|p103|||Of Hearty and O'Leary (2008). Invalid name apparently for part of Tamala Limestone, in Womerangee Hill area.||||||
70015|Woongara Rhyolite|61526|5|Briefly described|p879|||||||||
70015|Woongara Rhyolite|64728|6|Mentioned|p107.||||c.2450 Ma.|Unit in Hamersley Group.||||
70015|Woongara Rhyolite|71513|6|Mentioned|p66,|||Pilbara Craton. Interpreted to have been deposited in a back-arc setting.||Hamersley Group|||Felsic volcanic rocks (rhyolite).|
34322|Woongara volcanics|22701|5|Briefly described|Fig2,p39|Neoarchean|Neoarchean|Hamersley Group, Hamersley Basin. Overlies Weeli Wolli Iron Formation. Overlain by Boolgeeda Iron Formation. Probably misspelt.||||||07-NOV-08
33833|Woongarra Sequence|22546|4|Described|370|Paleoproterozoic||Geol province Turee Creek Basin. Overlain by Turee Creek Supersequence. U-Pb zircon age 2470 +/-30 Ma.||||||07-NOV-08
34376|Woongarra Supersequence|22682|5|Briefly described|Fig20,p29|Siderian|Siderian|2499-2452 Ma. See also Brockman Supersequence||||||03-MAR-10
81388|Woongarra rhyolite|70509|5|Briefly described|p31,32, 35|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. Referred to as Woongarra volcanics on p14, Fig1B.||Unit of Hamersley Group.||Overlain by Boolgeeda Iron Formation. Underlain by Weeli Wolli Formation.||16-AUG-19
29174|Woongarra volcanics|39200|6|Mentioned|p287|||||||||
29174|Woongarra volcanics|42148|6|Mentioned|p690|||||||||
32773|Wooramel "Stage"|45016|14|Not recorded|p64|||Ref.to Raggatt 1936.||||||
33006|Wooramel Sandstone|44344|14|Not recorded|opp.4. map|||This is the unit now known as Moogooloo Sandstone. (G50-1).||||||
33006|Wooramel Sandstone|44537|14|Not recorded|map legend||Artinskian|||||||
33006|Wooramel Sandstone|44657|14|Not recorded|p.5,7,9,17|||||||||
67850|Wooramel Suite""|24544|5|Briefly described|p6|||Superseded by Bertibubba Supersuite.||||||
34920|Wooramel suite|22904|6|Mentioned|p57 fig 1|||||||||16-JUL-08
34920|Wooramel suite|50218|6|Mentioned|p239|||Superseded by Bertibubba Supersuite.||||||07-FEB-11
34920|Wooramel suite|50219|6|Mentioned|p261|||Of Sheppard et al (1999).  Superseded by Bertibubba Supersuite.||||||07-FEB-11
34920|Wooramel suite|50220|6|Mentioned|p280|||Superseded by Bertibubba Supersuite.||||||
38578|Wooramel suite""|23781|6|Mentioned|p6|||Superseded by Bertibubba Supersuite.||||||
38669|Woorana syenite|23786|5|Briefly described|p35 Tb. 4|||Informal name. Geological Province: Yilgarn Craton.||||||
38749|Woroongunyah Formation|24025|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin.||||||
79820|Worrunga Formation|69586|5|Briefly described|p1|||Said to have been previously named the Vivien Metasediments. Crops out around the Mount White Syncline.|||||Feldspathic rocks.|
27019|Wright Hill beds|23282|6|Mentioned|p52,58,59|||Lower part may be equivalent to Alinya Formation.||||||
27019|Wright Hill beds|23287|6|Mentioned|Fig.2,4|||Age: Ediacarian. of Eastern Officer Basin.||||||
27019|Wright Hill beds|23288|6|Mentioned|Fig.5,18|||of Central Officer Basin.||||||
27019|Wright Hill beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27019|Wright Hill beds|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Siltstone, sandstone, quartzite, chert.||||||
27019|Wright Hill beds|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Siltstone, sandstone, quartzite and chert. Age and correlation very uncertain.||||||
27019|Wright Hill beds|61732|6|Mentioned|p63, p68|||Geological Province: Birksgate Sub-basin.||||||07-FEB-11
27019|Wright Hill beds|62453|5|Briefly described|p5 Fig. 3, 18|Cryogenian|Cryogenian|Geological Province: Officer Basin. Lateral equivalent to Lefroy Formation.||||||03-FEB-14
27019|Wright Hill beds|63397|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||18-JUL-07
27019|Wright Hill beds|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
27019|Wright Hill beds|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
27019|Wright Hill beds|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Punkerri Sandstone, Ungoolya Group (Rodda beds), Karlaya Limestone. Group description: Marine sandstone, grey indurated mudstone and limestone.||Ungoolya Group||Said to be equivalent to Wilpena Group||
27019|Wright Hill beds|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
27019|Wright Hill beds|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
27019|Wright Hill beds|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
27019|Wright Hill beds|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
70707|Wright Hill beds''|62453|6|Mentioned|p33|||Informal name.||||||
29434|Wungabai Limestone|42933|5|Briefly described|Fig.94 p258|||Misspelling of Wungabal Limestone of Mory & Beere (1988).||||||
40346|Wyloo Group Formations, Lower|24573|6|Mentioned|p670 Fig.1|||Geological Province: Pilbara Craton||||||
40348|Wyloo Group Formations, Upper|24573|6|Mentioned|p670 Fig.1|||Geological Province: Pilbara Craton||||||
40410|Wyloo Group, Lower|23612|6|Mentioned|p865|||Informal - see Wyloo Group.||||||
40410|Wyloo Group, Lower|24544|5|Briefly described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Unconformably ovelries Turee Creek Group. Unconformably overlain by Upper Wyloo Group. Geological Province: Ashburton Basin.||||||07-NOV-08
40410|Wyloo Group, Lower|24607|6|Mentioned|p967|||Informal - see the Wyloo Group. Geological Province: Ashburton Basin.||||||
40410|Wyloo Group, Lower|50227|5|Briefly described|p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Wyloo Group.  Age:2209Ma. See also p445.||||||07-FEB-11
40410|Wyloo Group, Lower|61276|4|Described|p578-580|Orosirian|Orosirian|Base age ~2045. Age: 2031 +/- 6Ma  from Wooly Dolomite, upper unit of Lower Wyloo Group.  Previous age interpretation: 2209 +/- 15Ma  from a sedimentary breccia, now reinterpreted as a provenance age.|||Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.|||17-OCT-16
40410|Wyloo Group, Lower|61526|5|Briefly described|p879|||Informal - see Wyloo Group. Includes Beasley River Quartzite and Cheela Springs Basalt. Unconformably overlain by Upper Wyloo Group.||||||
40410|Wyloo Group, Lower|63432|5|Briefly described|p735 Fig. 1|Proterozoic|Proterozoic|Geological Province: Pilbara Craton.||||||07-FEB-11
40410|Wyloo Group, Lower|67056|5|Briefly described|p419 Fig.2, pp422-425.|Paleoproterozoic|Paleoproterozoic|Up to 10-12 km thick. Predates ore formation and therefore could not contribute to martite-goethite ore burial.|||Includes Beasley River Quartzite, Cheela Springs Basalt and Wooly Dolomite.|Unconformably overlies the southern margins of the Mount Bruce Supergroup. Is overlain by Upper Wyloo Group with an increasing angular discordance toward the west.||
40410|Wyloo Group, Lower|67130|6|Mentioned|p3 fig 2, p5, p24 fig 17, p39|||Discontinued sub division. Ashburton Basin. Unconformably overlies Hamersley basin. Deposited as part of a clastic wedge during extensional basin formation.|2210  Ma - 2030 Ma||Includes Cheela Springs Basalt, Wooly Dolomite|Unconformably overlies Turee Creek Group, Unconformably overlain by Wyloo Group, Upper||
40410|Wyloo Group, Lower|67829|6|Mentioned|p451.|||||||||
40410|Wyloo Group, Lower|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Of Ashburton Basin.|||Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.||Conglomerate, sandstone, mudstone, basalt, chert, and locally stromatolitic dolomite.|
40410|Wyloo Group, Lower|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.|||Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.|||
40410|Wyloo Group, Lower|69596|5|Briefly described|p5-7, p8 Fig.5|Paleoproterozoic|Paleoproterozoic|Southern Pilbara. More often than not presented as (informal) lower Wyloo Group. ~3km thick. See also references to Wyloo Group (p1, p4, p7), and Upper Wyloo Group (p5, p8 Fig.5).|c.2208 Ma.||||Contains up to 2km thickness of fine-grained mafic rock (Cheela Springs Basalt), and coarse-grained siliciclastic sedimentary rocks.|
40410|Wyloo Group, Lower|69745|6|Mentioned|p269-273, 275-276, 287-289|||Hamersley Province.|||Cheela Springs Basalt; Beasley (River) Quartzite.|Unconformably overlies Turee Creek Group (Mount Bruce Supergroup). Is overlain unconformably by Upper Wyloo Group.||
40410|Wyloo Group, Lower|70327|6|Mentioned|p2-3, p17|||Horseshoe Basin.||Wyloo Group.||||
40410|Wyloo Group, Lower|70936|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province, Pilbara Craton.||||||
40410|Wyloo Group, Lower|71003|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||||||
40410|Wyloo Group, Lower|71550|5|Briefly described|p34-37,45|Rhyacian|Rhyacian|Geological province: Of Hamersley Basin.|||Includes Cheela Springs Basalt and Beasley River Quartzite.|Overlain by upper Wyloo Group.||03-SEP-19
40410|Wyloo Group, Lower|71808|6|Mentioned|p74, p86||||c. 2200 Ma|||Overlies the Turee Creek Group.||
40410|Wyloo Group, Lower|72447|6|Mentioned|p238|||||||||
40410|Wyloo Group, Lower|73538|6|Mentioned|p2 Fig. 1B, p4||||||Cheela Spring Basalt, Beasley River Quartzite, Wooly Dolomite|Unconformably underlain by the Turee Creek Group including the Kazput Formation.|Includes carbonates, mafic volcanics, and quartzite.|
40411|Wyloo Group, Upper|23612|5|Briefly described|p839 Fig 2|||Informal - see Wyloo Group.||||||
40411|Wyloo Group, Upper|24544|5|Briefly described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Lower Wyloo Group. Unconformably overlain by Capricorn Group. Geological Province: Ashburton Basin.||||||19-SEP-13
40411|Wyloo Group, Upper|24607|6|Mentioned|p967|||Informal - see the Wyloo Group||||||
40411|Wyloo Group, Upper|43561|6|Mentioned|Fig.5,p1436|||Variation on Wyloo Group||||||
40411|Wyloo Group, Upper|50227|5|Briefly described|p442, p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Wyloo Group.  Age: ca.1843Ma. See also p445.||||||07-FEB-11
40411|Wyloo Group, Upper|61276|4|Described|p577-580|Orosirian|Orosirian|Comprises: Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation.||||||17-OCT-16
40411|Wyloo Group, Upper|61526|5|Briefly described|p880|||Informal - see Wyloo Group. Composed of Mount McGrath Formation, Duck Creek Dolomite, Jume Hill Volcanics and Ashburton Formation. Unconformably overlies the Lower Wyloo Group.||||||27-JAN-06
40411|Wyloo Group, Upper|63432|5|Briefly described|p735 Fig. 1|Proterozoic|Proterozoic|Geological Province: Pilbara Craton.||||||07-FEB-11
40411|Wyloo Group, Upper|66882|6|Mentioned|p118|Statherian|Orosirian|Ashburton Basin, Pilbara Craton. Timing permits possible linkages with deposition of Cleve and Darke Peak Groups.|1840-1790 Ma|||||
40411|Wyloo Group, Upper|67056|5|Briefly described|p419 Fig.2, p422.|Paleoproterozoic|Paleoproterozoic||||Includes Mount McGrath and Ashburton Formations, Duck Creek Dolomite and June Hill Volcanics.|Overlies the Lower Wyloo Group with an increasing angular discordance toward the west.||
40411|Wyloo Group, Upper|67130|6|Mentioned|p3 fig 2, p5, p24 fig 17|||Discontinued sub division. Ashburton Basin. Unconformably overlain by sequences of the Blair, Bresnaha, Edmund and Collier basins.|1830 Ma - 1790 Ma||Includes Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation|Unconformably overlies Wyloo Group, Lower, Unconformably overlain by Bangemall Group||
40411|Wyloo Group, Upper|67827|5|Briefly described|p416 Fig.5, p426|Orosirian|Orosirian||~1.85 Ga-1800 Ma||Includes Mount McGrath Formation, Duck Creek Dolomite and June Hill Volcanics.|||
40411|Wyloo Group, Upper|67829|6|Mentioned|p451.|||||||||
40411|Wyloo Group, Upper|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Of Ashburton Basin.|||||Undivided; wacke, mudstone, ferruginous mudstone, banded iron-formation, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|
40411|Wyloo Group, Upper|69596|5|Briefly described|p5, p8 Fig.5|Paleoproterozoic|Paleoproterozoic|Ashburton Basin, Southern Pilbara. See also references to Wyloo Group (p1, p4, p7), and Lower Wyloo Group (p5-7, p8 Fig.5).|c.2030-c.1806 Ma.||||Siliciclastic and carbonate sedimentary rocks.|
40411|Wyloo Group, Upper|69745|6|Mentioned|p269-273, 275, 286-287, 289|||Hamersley Province.|c.2000 Ma.||Mount McGrath Formation.|Unconformably overlies Lower Wyloo Group. Is overlain unconformably by Bresnahan Group.||
40411|Wyloo Group, Upper|70936|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province, Pilbara Craton.||||||
40411|Wyloo Group, Upper|71003|6|Mentioned|p61|Paleoproterozoic|Paleoproterozoic|Pilbara Craton.||||||
40411|Wyloo Group, Upper|71550|6|Mentioned|p36|Paleoproterozoic|Paleoproterozoic|Geological province: Of Hamersley Basin.||||Underlain by lower Wyloo Group.||03-SEP-19
40411|Wyloo Group, Upper|71808|5|Briefly described|p86, p149||||||Includes the Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics and the Ashburton Formation.|||
40411|Wyloo Group, Upper|72447|6|Mentioned|p238|||||||||
40409|Wyloo Group, lower|22716|6|Mentioned|table4,p229|Paleoproterozoic|Paleoproterozoic|||||||
40409|Wyloo Group, lower|23280|6|Mentioned|p1084-6|||||||||
40409|Wyloo Group, lower|24544|5|Briefly described|p46 Fig.34|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Province.||||||07-NOV-08
40409|Wyloo Group, lower|24602|5|Briefly described|p855 Fig. 2|||Informal - see the Wyloo Group||||||
40409|Wyloo Group, lower|24607|6|Mentioned|p970|||Informal - see the Wyloo Group. Geological Province: Ashburton Basin.||||||
40409|Wyloo Group, lower|50216|6|Mentioned|p211 Fig.4|||Informal - see Wyloo Group||||||
40409|Wyloo Group, lower|50226|6|Mentioned|p415|||Informal - see Wyloo Group.||||||
40409|Wyloo Group, lower|61526|6|Mentioned|p882, p883|||Informal - see Wyloo Group.||||||
40409|Wyloo Group, lower|63866|6|Mentioned|p151, p154, p168, p175|||Ashburton Basin. Intruded by dolerite dykes with SHRIMP U-Pb Baddeleyite ages of 2009 +/- 16 Ma and 2007 +/- 16 Ma.||||||
40409|Wyloo Group, lower|66887|5|Briefly described|p20-21|||Ashburton Basin. Pilbara Craton.|||Cheela Springs Basalt|||
40409|Wyloo Group, lower|68035|5|Briefly described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. |~2421 - 2031 Ma||Includes Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.|||
40409|Wyloo Group, lower|69003|5|Briefly described|p4, p7-9, p24, p35|||Ashburton Basin.|||Beasley River Quartzite, Cheela Springs Basalt, Wooly Dolomite.|Overlies Turee Creek Group. Is overlain unconformably by upper Wyloo Group and Bresnahan Group.||
40409|Wyloo Group, lower|69028|5|Briefly described|Map Legend|Orosirian|Rhyacian|Ashburton and Blair Basins. These three Formations are mapped as a single unit. Geochronology by Muller et al. (2005), Martin et al. (1998), and Martin and Morris (2010).|2210-2030 Ma||Includes the Beasley River Quartzite, Cheela Springs Basalt, and Wooly Dolomite.||Includes conglomerate, sandstone, mudstone, basalt, chert, and locally stromatolitic dolomite.|07-MAY-14
40409|Wyloo Group, lower|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Obsolete name, replaced by the Shingle Creek Group.||||||
40409|Wyloo Group, lower|71169|6|Mentioned|p63|||||||||
40409|Wyloo Group, lower|73168|6|Mentioned|p765|Rhyacian|Rhyacian|Ashburton Basin. Detritus inferred to be sourced from Hamersley Group.|2215-2145 Ma|||||
40447|Wyloo Group, upper|22716|5|Briefly described|table4,p227,229|Orosirian|Orosirian|Age: 1840Ma. Marks the start of the Capricorn Orogeny.||||||
40447|Wyloo Group, upper|23280|6|Mentioned|p1084|||||||||
40447|Wyloo Group, upper|24544|5|Briefly described|p46 Fig.34|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Province.||||||07-NOV-08
40447|Wyloo Group, upper|24602|5|Briefly described|p853, p862|||Geological Province: Ashburton Fold Belt. Informal - see the Wyloo Group||||||
40447|Wyloo Group, upper|50216|6|Mentioned|p211 Fig.4|||Informal - see Wyloo Group||||||
40447|Wyloo Group, upper|50225|5|Briefly described|p388|Paleoproterozoic|Paleoproterozoic|Informal - see Wyloo Group. Intruded by Boolaloo Granodiorite.  Age: c.1806Ma.||||||07-FEB-11
40447|Wyloo Group, upper|50226|5|Briefly described|p415|||Informal - see Wyloo Group.||||||
40447|Wyloo Group, upper|61262|5|Briefly described|p444-5|||Informal name. Geological Province: Ashburton Basin. ||||||
40447|Wyloo Group, upper|61526|6|Mentioned|p882|||Informal - see Wyloo Group.||||||
40447|Wyloo Group, upper|63246|6|Mentioned|p479|||Informal - see Wyloo Group. Lower grade metasedimentary rocks.||||||
40447|Wyloo Group, upper|63866|6|Mentioned|p151, p154, p168, p175|||Ashburton Basin.||||||
40447|Wyloo Group, upper|66887|5|Briefly described|p2|||Pilbara Craton.|||Ashburton Formation|||
40447|Wyloo Group, upper|68035|5|Briefly described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. |~1.83 - 1.79 Ga||Includes Mount McGrath Formation, Duck Creek Dolomite, Ashburton Formation.|||
40447|Wyloo Group, upper|69003|5|Briefly described|p8, p9 Fig.9, p24-26, p35|||Ashburton Basin. Deposition was broadly synchronous with the Yapungku Orogeny. c.8km thick. Most sediments were sourced from the Glenburgh Terrane. Deformed between c.1806 Ma and 1786 Ma, as the Boolaloo Granodiorite crosscuts deformation fabrics.|c.1806 Ma.||Mount McGrath Formation, Duck Creek Dolomite, June Hill Volcanics, Ashburton Formation.|Unconformably overlies Wooly Dolomite (lower Wyloo Group) or Cheela Springs Basalt. Is intruded by Boolaloo Granodiorite. Is overlain unconformably by Bresnahan Group.||
40447|Wyloo Group, upper|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. These three Formations are mapped as a single unit.
|2030-1800 Ma.||Includes Mount McGrath Formation, Duck Creek Dolomite, and Ashburton Formation.||Includes wacke, mudstone, ferruginous mudstone, banded iron-formation, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|07-MAY-14
40447|Wyloo Group, upper|73168|6|Mentioned|p765|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Deposited in an extensive foreland basin system accompanying onset of the Capricorn Orogen.|||||Volcano-sedimentary rocks.|
40447|Wyloo Group, upper|73442|5|Briefly described|p3|||Pilbara Craton.|||||Wacke, mudstone, ferruginous mudstone, banded iron-formation, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|
72995|Wyman formation|63142|5|Briefly described|p487 Fig. 2|||Geological Province: Warrawoona Syncline. Felsic rocks.||||||29-MAR-07
41893|X Shale""|12758|6|Mentioned|p18, p46|||Informal reference to shale (Devereux, 1993) within the former Parmelia Formation - now part of the Carnac Formation.  See also p47 Fig. 50.||||||19-OCT-04
40481|X-mas Creek Member|24466|5|Briefly described|p386 Fig. 3|Permian|Permian|Abbreviation of Christmas Creek Member.||||||
41894|Y Shale""|12758|6|Mentioned|p18, p46|||Informal reference to shale (Devereux, 1993) within the former Parmelia Formation - now part of the Carnac Formation.  See also p47 Fig. 50.||||||19-OCT-04
24129|Yadgymurrin Conglomerate Member|40938|4|Described|p19|||||||||
78504|Yalgowra Mafic-Ultramafic Suite|68110|6|Mentioned|p674 Fig. 2|||Variation on Yalgowra Suite (p687).||||||10-OCT-14
39779|Yallingarintha Tonalite|24193|5|Briefly described|p894 Fig.1|Archean|Archean|Geological Province: Pilbara Craton. Of the Yule batholith. Age: ca. 3420Ma.||||||07-NOV-08
80542|Yamagee granite|70804|6|Mentioned|p31|||||||||
80500|Yamangee Granite|63866|5|Briefly described|p161|Orosirian|Orosirian|Yilgarn Craton. Intrudes early to late Archaean granitic gneiss, amphibolite and metasedimentary gneisses.|1958 +/- 4 Ma (SHRIMP U-Pb, Nelson, 1999)|||||
83156|Yamarna Group|72491|6|Mentioned|p5 Fig.4|||Burtville Terrane, Yilgarn Craton.||||||
29183|Yampi Member iron-formation|36003|6|Mentioned|Fig.5|||||||||
38168|Yampi Sandstone""|23722|6|Mentioned|p34|||Superseded - see Yampi Formation[?].||||||16-JUN-14
77525|Yandal Sequence|66880|6|Mentioned|p10, p18, p28. |Archean|Archean|There is a formally-named unit, the Yandal Sandstone. In this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank. Fluvial siliciclastic deposits in northern Gindalbie Terrane.|2680 +/- 6 Ma.|||||
77558|Yandal Supersequence|66936|5|Briefly described|p137, p149. |Archean|Archean|Gindalbie Terrane. Interpreted to be time-equivalent of Kurrawang Supersequence. At least 800 m thick. |||||Poorly-exposed, highly-deformed quartzosericitic sandstones.|
77558|Yandal Supersequence|66938|6|Mentioned|p187. |Archean|Archean|An axial (fluvial environment) system, with transport to the south or southeast, implying north to south paleoslopes. Depositional facies are characterisitic of high-discharge bedload draining areas of high relief.||||||
69026|Yandal greenstones|60978|6|Mentioned|p56, p58|||Geological Province: Yilgarn Craton||||||
38647|Yandal sandstone|23786|5|Briefly described|p24|||Informal name - see Yandal Sandstone.  Geological Province: Yilgarn Craton.||||||
29184|Yandanooka Beds""|36293|6|Mentioned|p52|||Refers Woolnough & Somerville 1924.||||||
29184|Yandanooka Beds""|36872|3|Fully described|p72|||Renamed Yandanooka Group||||||
73582|Yandearra Granodiorite|63441|5|Briefly described|p11 Tb. 2|Archean|Archean|Of Sisters Supersuite. Geological province: Pilbara Craton. On SATIRIST sheet. Within the Yule Granitic Complex.||||||07-FEB-11
76841|Yandicogina Shale Member|67025|6|Mentioned|p319.|||Typo for Yandicoogina Shale Member.||||||
80060|Yandicoogina Granodiorite|69167|5|Briefly described|169038.1.pdf|Archaean|Archaean|Age derived from sample of medium and even grained, unfoliated to weakly foliated granodiorite (169038.1.pdf). Analysed 2001.|3315 +/- 2 Ma (SHRIMP)|||||22-SEP-17
80060|Yandicoogina Granodiorite|69590|5|Briefly described|169038.1.pdf|||Of Mount Edgar granotoid Complex, East Pilbara Granote-Greenstone Terrane. Sample GSWA 169038 (bt-hl granodiorite) yielded an interpreted igneous crystallisation age of 3315+\-2 Ma for the granodiorite (weighted mean 207Pb/206Pb).||||||
35007|Yandicoogina Member|23045|5|Briefly described|289|||Parent Brockman Iron Formation||||||
35007|Yandicoogina Member|65757|5|Briefly described|p84 Fig.2|||Banded iron formation? Top of the Brockman Iron Formation, underlies the Weeli Wolli Formation, overlies the Joffre Member.||||||
38965|Yandigoogina Suite|23807|5|Briefly described|p126|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
38965|Yandigoogina Suite|24590|5|Briefly described|p67 Fig. 2.17, p68|Archean|Archean|Misspelt? See also Yandicoogina Suite. Trondhjemite-tonalite suite of Mount Edgar Granitoid Complex. Age: 3304+/-10Ma. Presented in combination with Boodallana Suite.||||||07-FEB-11
83184|Yandinilling dyke|73056|6|Mentioned|p292|Neoarchean|Neoarchean|Yilgarn Craton. NE-trending dyke, oldest known mafic dyke in Yilgarn Craton. Dated from one outcrop, probably part of larger dyke swarm across the South West Terrane. Yandinilling dykes p293 Fig.2, age of 2615 Ma.|ca. 2620 Ma||||Mafic dyke.|
83184|Yandinilling dyke|73057|5|Briefly described|p6, p8-9|Neoarchean|Neoarchean|Yilgarn Craton. Informal name. Oldest known mafic dyke in Yilgarn Craton. 2615+/-6 Ma ID-TIMS and 2610+/-25 Ma in situ SHRIMP ages are from baddeleyite from one dyke. May belong to a major dyke swarm indicated by NE-trending linear magnetic features. Basement rocks not exposed at outcrop, interpreted to intrude Archean metagranite from geological mapping.|2615+/-6 Ma ID-TIMS U-Pb, 2610+/-25 Ma SHRIMP U-Pb|Yandinilling dyke swarm|||Mafic dyke, includes dolerite with intergranular ophitic to sub-ophitic texture comprising 45-50% plagioclase, 35-40% pyroxene, up to 5% ilmenite and magnetite, 1-2% sulfides.|
83185|Yandinilling dyke swarm|73057|6|Mentioned|p1, p9-10|||Yilgarn Craton, southwest. Swarm of NE-trending dykes indicated by linear magnetic anomalies, potentially extends for hundreds of kilometres. The swarm is informally named after the one dated dyke and the terms are used interchangeably.|||Yandinilling dyke|||
74635|Yangibana ironstones|64329|6|Mentioned|p15, p20|||Alkaline igneous complex - part of Gifford Creek Complex; dykes occur 300km east-northeast of Carnarvon in Gascoyne Province of WA. The term "ironstones" derives from the fact that these dykes are ferrocarbonatite-magnetite-rare earth-bearing rocks.||||||29-JUL-08
74635|Yangibana ironstones|74494|5|Briefly described|p1010, p1023|||Alteration phase associated with primary rocks of the Gifford Creek Carbonatite Complex. Monazite enrichment in REE is interpreted to have occurred through eluvial supergene processes. Precursor is likely ankerite-siderite carbonatite, underwent Rodberg-style alteration followed by weathering and oxidation by meteoric water.||Gifford Creek Carbonatite Complex||||
37098|Yardanunyah Formation|23746|6|Mentioned|p26|||Misspelt - see Yandanunyah Formation.||||||
37098|Yardanunyah Formation|24025|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin.||||||
25664|Yardarino Sandstone""|23816|5|Briefly described|p235|Late Permian|Late Permian|Max. thickness: 23  m. Of the Wagina Sandstone. Also referred to as the "Basal Triassic Sandstone".||||||
25664|Yardarino Sandstone""|31910|6|Mentioned|p18|||Refers Playford & Low (1972)||||||
25664|Yardarino Sandstone""|36293|6|Mentioned|p111|||See also P123.||||||
25664|Yardarino Sandstone""|36890|6|Mentioned|p235|||Renamed Yardarino Sandstone Member.||||||
79424|Yareweeree Member|67201|6|Mentioned|p21 Fig.12|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Mallina Basin. [shortened variation of Yareweeree Boninite Member]||Bookingarra Formation||||
67832|Yaringa Evaporite|1943|2|Defined|p383-p384, p373, p375 Fig.3, p376 Fig 4|Ludlow|Wenlock|Type section in Yaringa-1, 1194.8-1271m. Limited known distribution. See Fig. 2. Age probably Wenlock to Ludlow, from spores and fragmentary conodonts. Max. thickness: 145m in Tamala-1 (726-871m). Formerly Yaringa Evaporite Member (Playford et al. 1975) and equivalent to Unit B of Hocking et al. (1987).||Dirk Hartog Group||Overlies Ajana Formation apparently conformably. Gradational contact with overlying Hamelin Formation.|Laminated oolitic dolostone interbedded with saliferous dark grey shales, halite beds and anhydrite.|
67832|Yaringa Evaporite|23935|5|Briefly described|p19|||Superseded by the Yaringa Formation. Geological Province: Southern Carnarvon Basin.||||||
73994|Yaringa Halite|14227|5|Briefly described|Enclos. 2|Llandovery|Llandovery|Probably informal name for Yaringa Formation. Age is Late Llandovery. See Yaringa Formation.||||||07-FEB-11
79284|Yarlarweelor Complex|65692|5|Briefly described|p24|||Narryer Terrane. Mentioned as being of a comparable age to, and hence possible source of, the oldest (3125 +/- 17 Ma) detrital zircon in the Chiall Formation in the Earaheedy Basin.|3300 Ma maximum (Nutman et al., 1993).|||||
79284|Yarlarweelor Complex|66106|6|Mentioned|p27, 44|||Narryer Terrane, Yilgarn Craton.||||||
69733|Yarlarweelor Gneiss Complex, lower|24332|5|Briefly described|p149 Fig. 11a|Paleoproterozoic||Informal - see Yarlarweelor Gneiss Complex.  Age: 1812Ma.||||||07-NOV-08
36894|Yarlarweelor gneiss complex|23485|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Informal.  Geological Province: Yilgarn Craton.||||||07-NOV-08
36894|Yarlarweelor gneiss complex|23525|5|Briefly described|p2 Fig. 1|Orosirian|Archean|Age: 3300-1800Ma||||||07-NOV-08
36894|Yarlarweelor gneiss complex|23592|4|Described|p3 + p4|Archean|Archean|Informal name.||||||07-NOV-08
41210|Yarlaweelor Complex|50222|6|Mentioned|p327|||Misspelt - see Yarlarweelor Gneiss Complex.  See also Yarlaweelor Gneiss Complex.||||||23-JUN-04
41211|Yarlaweelor Gneiss Complex|50222|6|Mentioned|p316 Fig. 1|Paleoproterozoic|Paleoproterozoic|Misspelt - see Yarlarweelor Gneiss Complex.  See also Yarlaweelor Complex.||||||07-NOV-08
70184|Yarrabubba Granite|61560|5|Briefly described|p493|Archean|Archean|Displays shatter cones and petrographic indicators in quartz within outcrops, evidence of the Yarrabubba impact structure in the Yilgarn Craton. Intruded by the Barlangi Granophyre. Age: 2.65Ga. ||||||07-NOV-08
70184|Yarrabubba Granite|61564|5|Briefly described|p593, p594 Fig. 7|Proterozoic|Proterozoic|Hosts the Yarrabubba impact structure. Shocked granitic rocks of Yarrabubba Granite displaying classic shatter cones and pseudotachylite veins surround the Barlangi Granophyre. ||||||
70184|Yarrabubba Granite|64771|5|Briefly described|p28-32|Neoarchaean|Neoarchaean|Yarrabubba Impact Structure. Contains impact evidence including shatter cones, planar deformation features in quartz, pseudotachylites and impact breccias. Contains sills of Barlangi Granophyre which were melted by impact.|c.2.7-2.6 Ga.||||Pale pink, medium- to coarse-grained monzogranite, consisting of quartz, albitic plagioclase and microcline, with subordinate muscovite and biotite. Mineralogy and microstructure described. Numerous 'pseudotachylite' dykes.|
70184|Yarrabubba Granite|70830|5|Briefly described|p14-p15, p18||||||||Pale pink, medium- to coarse-grained monzongranite consisting of quartz, albitic plagioclase and microcline with subordinate muscovite and biotite.|
70190|Yarrabubba granite|61564|6|Mentioned|p595 Fig. 8|||Informal - see Yarrabubba Granite. ||||||
39302|Yarragadee Coal Measures|24374|5|Briefly described|p8|||Probably an informal unit within Yarragadee Formation. Geological Province: Perth Basin.||||||
74687|Yarraloola Congomerate|64580|4|Described|map legend||Early Cretaceous|Misspelling of Yarraloola Conglomerate. Cobble to boulder conglomerate.||||||15-DEC-08
74687|Yarraloola Congomerate|69185|4|Described|GEOL_LUT_CSV files||Early Cretaceous|Of Northern Carnarvon Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|||||Poorly sorted sandstone (in places glauconitic), cobble to boulder conglomerate, and siltstone|
32759|Yarramulla Beds|45015|4|Described|p18||Proterozoic|Regionally metamorphosed sediments, mainly phyllite, with some slate and altered greywacke. Unconformably overlain by Badgeradda Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
79821|Yarraquin tonalite|69586|6|Mentioned|p21 Fig.20|||Informal name. Part of the Yarraquin Pluton [not a stratigraphic name]. Also appears as Yarraquin tonalites.|||||Tonalitic gneiss.|
72415|Yarrawolya Formation, lower|48823|6|Mentioned|p23|||Informal - see Yarrawolya Formation.||||||16-AUG-06
81311|Yarri granite|70020|6|Mentioned|p122|||Geological province: Eastern Goldfields Superterrane, Yilgarn Craton.||||||
29190|Yellow Drum dolostone|41730|6|Mentioned|p471|||||||||
69146|Yellow Drum formation|61139|5|Briefly described|p41|Early Carboniferous|Early Carboniferous|Geological Province: Canning Basin.||||||09-JUN-05
39304|Yellowdrum Dolomite|24377|6|Mentioned|P13|||Geological Province: Canning Basin||||||02-MAR-05
39292|Yellowdrum Formation|24246|5|Briefly described|p10|Famennian|Famennian|Overlies Nullara Limestone. Geological Province: Canning Basin.||||||
39292|Yellowdrum Formation|24370|5|Briefly described|p39|Early Carboniferous|Early Carboniferous|Geological Province: Canning Basin.||||||
39292|Yellowdrum Formation|24377|5|Briefly described|p13|Tournaisian|Tournaisian|Geological Province: Canning Basin||||||02-MAR-05
39305|Yellowdrum Upper Dolomite|24377|5|Briefly described|p13|||Informal name - see Yellowdrum Dolomite. Geological Province: Canning Basin||||||02-MAR-05
41222|Yelma formation|50223|6|Mentioned|p346|||Informal - see Yelma Formation.||||||23-JUN-04
37154|Yeneena Group""|23760|6|Mentioned|p21|Proterozoic|Proterozoic|Renamed Yeneena Supergroup. Geological Province: Yeneena Basin.||||||
37154|Yeneena Group""|24025|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Replaced by Yeneena Supergroup.  Geological Province: Pilbara Craton.||||||
37154|Yeneena Group""|50008|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|||||||
37154|Yeneena Group""|50228|5|Briefly described|p482|||Of Williams (1990). Replaced by Tarcunyah, Throssell and Lamil groups.||||||
37097|Yeneena Subgroup|23746|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
36911|Yeneena Supergroup""|23602|6|Mentioned|p15|||||||||
25670|Yeneena group|37214|6|Mentioned|p6|||||||||
30240|Yerrida Group|7471|5|Briefly described|p4,p8, Map legend|Proterozoic|Proterozoic||||Includes Windplain and Mooloogool Subgroups.|||
30240|Yerrida Group|12099|4|Described|p675-8, 680-1, 683,685-6, Figs.1,2,4,5,8|Statherian|Paleoproterozoic|New or redefined unit by Occhipinti et al. (1997). Unconformably overlies Yilgarn Craton and in fault contact with Marymia Inlier. Deposited in a continental setting. Minimum age given by Pb-Pb date on Pb mineralisation in the upper Juderina Formation.|Minimum age ~1650 Ma.||Includes Woodplain and Moologool Subgroups.|Unconformably overlain by Earaheedy Group. Thrust over by Bryah Group along the Goodin Fault.||04-MAR-13
30240|Yerrida Group|22501|5|Briefly described|p117|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|22694|4|Described|p7|||Glengarry Basin||||||
30240|Yerrida Group|22695|5|Briefly described|map|Proterozoic|Proterozoic|||||||
30240|Yerrida Group|22696|5|Briefly described|map|Proterozoic|Proterozoic|||||||
30240|Yerrida Group|22697|5|Briefly described|map|Proterozoic|Proterozoic|||||||
30240|Yerrida Group|22698|5|Briefly described|map|Proterozoic|Proterozoic|||||||
30240|Yerrida Group|22716|6|Mentioned|table4, p229|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|22903|6|Mentioned|63 fig 1|||||||||
30240|Yerrida Group|22940|5|Briefly described|Fig.1 p3|||See also Table 2 p12.||||||
30240|Yerrida Group|23151|5|Briefly described|p64|||||||||
30240|Yerrida Group|23413|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Yerrida Basin||||||
30240|Yerrida Group|23485|6|Mentioned|p16|||||||||
30240|Yerrida Group|23525|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|23529|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin||||||07-NOV-08
30240|Yerrida Group|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin||||||07-NOV-08
30240|Yerrida Group|23581|5|Briefly described|Map legend||Paleoproterozoic|In the Yerrida Basin||||||07-NOV-08
30240|Yerrida Group|23586|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23589|3|Fully described|p15|Paleoproterozoic|Paleoproterozoic|Age: 2200-1900 Ma. Overlain by Earaheedy Group. Geological Province: Yerrida Basin.||||||10-JUN-09
30240|Yerrida Group|23592|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological Province: Yilgarn Craton.||||||07-NOV-08
30240|Yerrida Group|23593|4|Described|p6|Statherian||Minimum Age: 1785+/-11 Ma (SHRIMP U-Pb zircon of the overlying Earaheedy Group). Overlying unit Earaheedy Group. Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|23597|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: 2173+/-64 Ma. Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23600|4|Described|p5|Proterozoic|Proterozoic|Overlying unit Earaheedy Group. Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Age: 2200 Ma. See also page 33 Appendix 1. Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23744|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Age: ~2250-1900 Ma (Pb-Pb isochron). Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23747|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Age: 2250-1800 Ma. Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|23749|4|Described|p6|Proterozoic|Proterozoic|Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|23759|4|Described|p15|Paleoproterozoic|Paleoproterozoic|See page 5 Fig 3. Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23781|6|Mentioned|p61|||Formerly "Glengarry Group".||||||
30240|Yerrida Group|23865|5|Briefly described|p169|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|23890|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|24017|5|Briefly described|p3 Fig. 1|||Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|24021|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin||||||07-NOV-08
30240|Yerrida Group|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Yerrida Basin.||||||07-NOV-08
30240|Yerrida Group|24183|6|Mentioned|p2 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
30240|Yerrida Group|24535|4|Described|p22|Paleoproterozoic|Paleoproterozoic|Deposited between 2200 and 1840 Ma. Has been thrust over by Bryah Group. Geological Province: Yerrida Basin. Maximum age based on Pb/Pb age of 2173 +/-63 Ma for stromatolitic carbonate at the base of the Windplain Subgroup|||Includes Windplain Subgroup?|||26-NOV-13
30240|Yerrida Group|24544|5|Briefly described|p38|||Previously of the "Glengarry Group".||||||
30240|Yerrida Group|43561|6|Mentioned|p1433|||||||||
30240|Yerrida Group|43831|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|43836|5|Briefly described|Map Legend||Proterozoic|||||||
30240|Yerrida Group|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Subdivided into Windplain and Mooloogool Subgroups.||||||18-MAY-04
30240|Yerrida Group|43843|5|Briefly described|Map Legend||Proterozoic|||||||
30240|Yerrida Group|44204|5|Briefly described|Map Legend||Proterozoic|||||||
30240|Yerrida Group|44830|5|Briefly described|Map Legend||Proterozoic|||||||
30240|Yerrida Group|44867|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|49893|4|Described|p3 Tb.1, p8|Proterozoic|Proterozoic|Overlain by the Earaheedy Group. Geological Province: Yerrida Basin. Age: ~2100-2200 Ma. Parts of this group formerly included in the Glengarry Group of Gee and Grey (1993). See also p2 Fig.1.||||||
30240|Yerrida Group|49896|5|Briefly described|p3 Tb. 2|||Includes lower units within lower Glengarry Gp - Maraloou, Killara, Doolgunna, Thaduna, Johnson Cairn and Juserina Formations; and former Finlayson Fm. Along with Bryah Gp, now supersedes Glengarry Gp. Subdivided into Mooloogool and Windplain Subgroups||||||
30240|Yerrida Group|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Comprises Windplain and Mooloogool Subgroups.  Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|50188|5|Briefly described|p2 Fig. 1|||Geological Province:  Yerrida Basin.||||||16-JUL-08
30240|Yerrida Group|50218|6|Mentioned|p242 Fig. 4|||||||||07-FEB-11
30240|Yerrida Group|50221|5|Briefly described|p296 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: <2300 Ma.||||||07-NOV-08
30240|Yerrida Group|50222|5|Briefly described|p321, p335|||Formerly subdivided into Windplain and Mooloogool Subgroups which are now upgraded to group status.  Yerrida Group is now abandoned.||||||
30240|Yerrida Group|50223|6|Mentioned|p345 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30240|Yerrida Group|50224|5|Briefly described|p368 Tb.1, p369 Fig. 1|Paleoproterozoic|Paleoproterozoic|Unconformably underlies the Yelma Formation (Tooloo Subgroup).||||||07-FEB-11
30240|Yerrida Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
30240|Yerrida Group|50226|6|Mentioned|p424 Fig. 5|||Geological Province: Yerrida Basin.||||||
30240|Yerrida Group|61269|6|Mentioned|p86 Fig.1|||||||||
30240|Yerrida Group|61271|6|Mentioned|p104|||||||||
30240|Yerrida Group|62289|4|Described|plate 1, p3 Fig. 1, p7 Fig. 3, p6-28|Palaeoproterozoic|Palaeoproterozoic|Parts outcrop in the former Glengarry Group (Basin) defined by Gee and Grey (1993); includes Windplain and Mooloogool Subgroups; faulted contact with Bryah Group; unconformably overlain by Earaheedy Group; unconformably overlies, or is in tectonic contact with, Archaean granite-greenstone rocks of Yilgarn Craton and Marymia and Goodin Inliers; Age: 2.2 to 1.9 Ga.||||||
30240|Yerrida Group|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.|||Includes Mooloogool Subgroup and Windplain Subgroup.|||14-APR-11
30240|Yerrida Group|63866|5|Briefly described|p165|||Yerrida Basin.|||Includes the Windplain Subgroup and the Mooloogool Subgroup.|Unconformably overlain by the Earaheedy Group.||
30240|Yerrida Group|64284|5|Briefly described|p58 Fig. 1, p61|||Geological Province: Yerrida Basin.||||||07-FEB-11
30240|Yerrida Group|64285|5|Briefly described|p67 Fig. 2|||Geological province: Yerrida Basin.||||||07-FEB-11
30240|Yerrida Group|64724|5|Briefly described|p43, p45 Fig.5|Orosirian|Orosirian|Yerrida Basin unit. Age an estimate as accurate geochronological data for this unit is limited.||||||
30240|Yerrida Group|64728|6|Mentioned|p94 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||Is unconformably overlain by Bangemall Supergroup.||
30240|Yerrida Group|64772|6|Mentioned|p20-21 Fig.10|Proterozoic|Proterozoic|||||||
30240|Yerrida Group|65264|5|Briefly described|p8 Fig.3, p26, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Contains the Windplain and Mooloogool Subgroups. Age: 2200Ma. Geological province: Yerrida Basin. See also p44 Appdx. 1.||||||07-FEB-11
30240|Yerrida Group|65408|5|Briefly described|pp81 - 85.|Paleoproterozoic|Rhyacian|Depositional age from basal Juderina Formation.|2258 +/- 180 Ma Pb-Pb isochron, Juderina Fm||Comprises Windplain and Mooloogool Subgroups.|Thrust under Bryah Group. Is unconformably overlain by Earaheedy Group.||18-NOV-11
30240|Yerrida Group|65411|5|Briefly described|p88.|Paleoproterozoic|Paleoproterozoic|Yerrida Basin. Rocks of this unit and Bryah Group were formerly of the Glengarry Group (abandoned).|||Includes Windplain and Mooloogool Subgroups; Finlayson Member.|||
30240|Yerrida Group|65412|6|Mentioned|pp96-103.|Paleoproterozoic|Paleoproterozoic||||Includes Windplain and Mooloogool Subgroups.|||
30240|Yerrida Group|65419|2|Defined|pp1-2, p4 Fig.1, pp6-7, p10 Fig.3.|Paleoproterozoic|Paleoproterozoic|Yerrida Basin. Named after Yerrida Spring. Type area is Glengarry and Peak Hill 1:250 000 sheets. Rocks of this unit were formerly included in the east and southeast Glengarry Group in the (eastern) Glengarry Basin, both terms now obsolete. Estimated total thickness c.6 km. Age constrained by over- and under-lying units.|Between 2.25 and 1.8 Ga.||Includes Windplain and Mooloogool Subgroups.|Is complexly faulted against the Bryah Group. Is unconformably overlain by the Earaheedy Group.|Terrigenous clastic rock, wacke, carbonate, evaporite; and volcaniclastic, mafic volcanic and intrusive rocks.|
30240|Yerrida Group|65472|6|Mentioned|p5 Fig. 4|||Yerrida Basin.||||||
30240|Yerrida Group|65692|6|Mentioned|p69|||The Capricorn Orogeny is considered (Pirajno et al., 2004) to have thrust the Bryah and Padbury Basins units over the lower part of this Group.||||||
30240|Yerrida Group|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Yerrida Basin. Includes Finlayson Member of Juderina Formation at its base, Johnson Cairn Formation above. Age shown as <2200 Ma.||||||
30240|Yerrida Group|65913|5|Briefly described|p2 Fig.1, p5|Paleoproterozoic|Paleoproterozoic|Rocks of this Group are undeformed or weakly deformed, and essentially unmetamorphosed.|||Includes Windplain and Mooloogool Subgroups.|Is unconformably overlain by Earaheedy Group.|Succession of sedimentary and igneous rocks.|24-MAY-16
30240|Yerrida Group|66299|6|Mentioned|p57.|||Formerly part of Glengarry Group (Daniels 1975). Once thought to be equivalent to metasediments of Moogie Metamorphics.||||||
30240|Yerrida Group|66427|6|Mentioned|p41 Tb.1, p43 Fig.2||||||Includes Windplain Subgroup.|||
30240|Yerrida Group|67269|6|Mentioned|p20-21 Fig.19|||Yerrida Basin.|||Juderina Formation.|||
30240|Yerrida Group|68561|5|Briefly described|GLENGARY_GEOLOGYP_LUT.csv||Proterozoic|Yerrida Basin. [Obsolete name, also used in 2_5M_GEOLOLYP98_LUT]||||||
30240|Yerrida Group|69003|6|Mentioned|p14|Paleoproterozoic|Paleoproterozoic|Deformed Palaeoproterozoic rocks; basement to Earaheedy Basin.||||||
30240|Yerrida Group|69080|6|Mentioned|p684|||Variably deformed low-grade metasedimentary rocks.||||||
30240|Yerrida Group|70153|5|Briefly described|142863.1.pdf||||||Includes Killara Formation.|||
30240|Yerrida Group|70796|5|Briefly described|glengarry_100k_geologyp_lut.csv|||Yerrida Basin. See also glengarry_500k_interpgeop_lut.csv, 118990.1.pdf, Glengarry100_2645_stratig.pdf.|||Includes the Windplain Subgroup, Mooloogool Subgroup.|||
30240|Yerrida Group|70804|5|Briefly described|p1-p4, p6, p16, p19|Palaeoproterozoic|Palaeoproterozoic|Makes up the eastern part of the former 'Glengarry Basin'. See also p21-p24, p26-p27, p37-p38.|c. 2174 Ma||Includes the Windplain and Mooloogool Subgroups.|Faulted against the Bryah Group.||
30240|Yerrida Group|70814|6|Mentioned|p48|||Yerrida Basin.||||||
30240|Yerrida Group|71042|6|Mentioned|p66 fig 2, p98|||||||||24-MAY-19
30240|Yerrida Group|71484|6|Mentioned|p122,125|||||||||30-AUG-19
41212|Yerrida Group, lower|22716|5|Briefly described|p229|Paleoproterozoic|Paleoproterozoic|||||||
41212|Yerrida Group, lower|50222|5|Briefly described|p333 Tb. 2|||Informal name for Windplain Group, formerly the Windplain Subgroup of the former Yerrida Group.||||||
34407|Yerrida Group, upper|22716|5|Briefly described|p229|Paleoproterozoic|Paleoproterozoic|Deposited in the Mooloogool rift.||||||06-AUG-15
39780|Yigalong granitoid|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton. Yigalong should probably be spelt Yilgalong.||||||07-NOV-08
26247|Yilgalong Granite|22953|6|Mentioned|Fig1p3|||||||||
26247|Yilgalong Granite|31308|6|Mentioned|Fig. 36|||||||||
26247|Yilgalong Granite|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26247|Yilgalong Granite|39426|2|Defined|Table 1|Archean|Archean|||||||07-NOV-08
26247|Yilgalong Granite|39697|3|Fully described|p48|||||||||
26247|Yilgalong Granite|44150|6|Mentioned|p130-131 Fig.2-130, p152|||||||||
26247|Yilgalong Granite|65829|6|Mentioned|p8.|||Hickman (1983). Superseded by Yilgalong Granitic Complex.||||||
74688|Yilgalong Granitic Complex|63854|5|Briefly described|p241. |Archean|Archean|Source of only some zircons (dated c.3290 Ma) in basal Mosquito Creek Formation.||||||
74688|Yilgalong Granitic Complex|64580|4|Described|map legend|Mesoarchean|Paleoarchean|Monzogranite and syenogranite, well foliated.||||||15-DEC-08
74688|Yilgalong Granitic Complex|65825|4|Described|p1, p6, p10, p21, p25. |Archean|Archean|Hosts the Boodalyerrie gold mining centre.|c.3291 - 3274 Ma (Nelson 2005).|||Intrudes Euro Basalt. Is overlain nonconformably by Fortescue Group.|Strongly deformed, fine- to medium-grained, biotite granodiorite and biotite monzogranite; local tonalite; pegmatite zones, quartz veins and mafic dykes common; occasional thin aplite dykes; small areas of weakly foliated leucocratic granodiorite.|
74688|Yilgalong Granitic Complex|65827|6|Mentioned|p26, p41|Paleoarchean|Paleoarchean|Bulk of this complex is in the 3292-3290 Ma range.
||||||
74688|Yilgalong Granitic Complex|65829|4|Described|p1, p6, pp8-10, p26. |Paleoarchean|Paleoarchean|Outcrops as low hills, rock outcrop and pavement. Was a basement high during deposition of the Fortescue Group; all its rocks dip away from the Complex to the west and north.|3292 - 3255 Ma.|||Intrudes Euro Basalt. Intruded by Cleland Supersuite. Is overlain nonconformably by the Fortescue Group.||
74688|Yilgalong Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
74688|Yilgalong Granitic Complex|69167|6|Mentioned|178008.1.pdf|Archaean|Archaean|Ages derived from samples of leucocratic monzogranite and biotite-muscovite tonalite (178089.1.pdf, 178008.1.pdf) (Structural?)|3274 +/- 5 Ma -3292 +/- 4 Ma (SHRIMP)|||||
74688|Yilgalong Granitic Complex|69792|6|Mentioned|p1100|||||||||
74688|Yilgalong Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
37860|Yilgalong Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
37860|Yilgalong Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
37860|Yilgalong Granitoid Complex|24188|6|Mentioned|p788 Fig.1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
37860|Yilgalong Granitoid Complex|24550|5|Briefly described|p30|||Comprises mainly metasediments.||||||07-FEB-11
37860|Yilgalong Granitoid Complex|44150|5|Briefly described|p147 Tb.2-21|||500 sq. km.|||||Biotite monzogranite, syenogranite, augen gneiss.|
37860|Yilgalong Granitoid Complex|50287|5|Briefly described|Map Legend|Archean|Archean|Age: c. 3258 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton.||||||07-NOV-08
37860|Yilgalong Granitoid Complex|61264|5|Briefly described|p63 Fig. 1|||Geological Province: Pilbara Craton.||||||
37860|Yilgalong Granitoid Complex|65008|6|Mentioned|p3 Fig.1|||Kurrana Terrane.||||||
37860|Yilgalong Granitoid Complex|65828|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane.|c.3292 Ma (Nelson 2005).||||Biotite monzogranite and granodiorite, foliated, metamorphosed; feldspar porphyry dyke, metamorphosed.|
77569|Yilgangi Supersequence|66937|5|Briefly described|p155, pp162-166.|Archean|Archean|Kalgoorlie Terrane. Thickness to 1335 m. Depositional sequences are identical with those in lower Penny Dam Supersequence. Interpreted as density-flow processes on submarine-canyon and linear-fan depositional systems.|||||Conglomerates, massive and clast-rich to stratified and matrix-rich; clasts change upward from basalt-dominant to polymict; lenticular interbeds of plane-bedded coarse- to medium-grained quartzolithic sandstone.|
77569|Yilgangi Supersequence|66938|6|Mentioned|p187. |Archean|Archean|Amalgamated depositional sequences are aggradationally up to progradationally stacked, implying uplift and sediment flux were outpacing tectonic escape.||||||
36948|Yilgangi conglomerate|23584|6|Mentioned|p10|||||||||
36948|Yilgangi conglomerate|24135|6|Mentioned|p41|||Informal name.||||||
36948|Yilgangi conglomerate|24174|5|Briefly described|p39|||Informal name.  Geological Province: Eastern Goldfields.||||||
36948|Yilgangi conglomerate|24196|5|Briefly described|p44|Archean||Minimum age of 2662 +/- 5 Ma provided by a monzodiorite dyke that intrudes the unit.||||||07-NOV-08
36948|Yilgangi conglomerate|60076|5|Briefly described|p12 Tb. 2|||Probably an informal name.  Local boulders, lithic wacke interlayers.  Max. thickness: >200m.  In the Edjudina-Laverton greenstones area.  See also p21.||||||02-FEB-05
77526|Yilgangie Sequence|66880|5|Briefly described|p18, p28. |Archean|Archean|This may be an informal variation of Yilgangi (sic) Conglomerate; in this study, the term "Sequence" seems to be used as an alternative to any other lithology/rank. |2676 +/- 7 Ma and 2664 +/- 4 Ma.|||Intruded by a granodiorite porphyry.|Includes sandstone.|
25673|Yilgarn System|33558|4|Described|p156|||||||||
29193|Yilgarn-Kalgoorlie Series""|35595|6|Mentioned|p3|||||||||
32619|Yilgarn-Kalgoorlie System|44316|14|Not recorded|map legend||Archean|||||||07-NOV-08
32619|Yilgarn-Kalgoorlie System|46316|14|Not recorded|p.6,15||Archean|Now called Coolgardie-Kalgoorlie Metamorphics, map,Tb.1, opp.p.6.||||||07-NOV-08
40747|Yilgatherra Sandstone Member|24183|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Superseded by the Yilgatherra Formation.||||||
42396|Yindagindy Limestone""|23815|6|Mentioned|p277|||Superseded by Yindagindy Formation (Condon, 1954). Geological Province: Carnarvon Basin.||||||
32617|Yindarlgoorda Series|46316|14|Not recorded|p.6,8||Archean|Correlated with rocks of the Coolgardie-Kalgoorlie Metamorphics. Tb.1 opp.p.6, p.8.||||||07-NOV-08
70185|Yingundji formation""|61560|5|Briefly described|p490|||Informal name. Undeformed sedimentary rocks situated within the ring of Liverpool Breccia around the Liverpool impact crater.  These rocks are probably a correlative of Buckingham Bay Sandstone of the basal Arafura Basin succession. ||||||
74099|Yinnetharra Gneiss|24197|6|Mentioned|p69|||Of Williams (1986). Informally referred to as the Yinnetharra Gneiss dome, parts of which are incorporated into the Minnie Creek Supersuite. Probably misspelt - place name is Yinnietharra Bore in WA.||||||07-FEB-11
74099|Yinnetharra Gneiss|66299|6|Mentioned|p249.|||Used in the term Yinnetharra Gneiss Dome (Williams 1986), an informal name for the distinctive Davey Well Granite.||||||
74099|Yinnetharra Gneiss|67855|6|Mentioned|p202|||See also Yinnetharra Gneiss Dome p201.||||||
41241|Yinnetharra pegmatites|50226|6|Mentioned|p418|||Not intended as a formal name.  Within the Gascoyne Complex.||||||
41358|Yinnietharra Granite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Minnie Creek Supersuite. See also the variation (probably misspelt) Yinnetharra Gneiss where referred to as a gneiss dome (p69).||||||07-FEB-11
41358|Yinnietharra Granite|50425|5|Briefly described|p1.3, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Minnie Creek Supersuite.||||||07-NOV-08
75109|York Granite|64769|6|Mentioned|p118, p119, p119 Fig. 117|||Name for dimension stone.||||||21-APR-09
72760|Youanmi Group|61909|5|Briefly described|p149 Fig.1|||In the Murchison district, W.A.||||||
24600|Youanmi Intrusion|39347|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
24600|Youanmi Intrusion|46313|2|Defined|p58|Archaean|Archaean|Of Stewart et al (1983). Co-magmatic with Windimurra Intrusion 15km to the northwest.  Comprises numerous layers up to 10m thick, of gabbro, leucogabbro, norite, melagabbro, pyroxenite, anorthosite and magnetite. Type locality included.||||||25-JUN-09
24600|Youanmi Intrusion|61909|6|Mentioned|p149|||Informal - see Youanmi Group.||||||
38609|Younger Granites""|23784|6|Mentioned|p42 Fig. 17|||Informal reference to the younger granites of the Yule Granitoid Complex.||||||
83394|Younger Greenstone Formation|73391|6|Mentioned|Appendices. A2 Table 3.1|||Gustafson and Miller (1937). Regional stratigraphic correlation chart of other workers.|||||Quartz dolerite, gabbro, hornblendite.|02-JUL-22
32574|Younger Greenstone Series|45473|14|Not recorded|p.80|||||||||
32574|Younger Greenstone Series|73391|6|Mentioned|Appendices. A2 Table 3.1|||McMath et al. (1953). Regional stratigraphic correlation chart of other workers.|||||Metagabbros and dolerites.|02-JUL-22
32618|Younger Greenstones""|46316|14|Not recorded|p.10||Archean|Map, Tb.1, p.10. Folded coarse grained amphibolites.||||||07-NOV-08
39191|Younger"" Ascot Formation|23768|6|Mentioned|p57, p76, p136|Early Pleistocene|Early Pleistocene|Geological Province: Perth Basin.  See also "younger" Ascot Formation.||||||10-MAR-05
74678|Yule Granitic Complex|63538|6|Mentioned|p10|Archean|Archean|Geological Province: Pilbara Craton.||||||07-FEB-11
74678|Yule Granitic Complex|64405|5|Briefly described|p2 Fig. 1|||||||||07-FEB-11
74678|Yule Granitic Complex|64580|4|Described|map legend||Paleoarchean|Granitic rock; metamorphosed.||||||05-NOV-08
74678|Yule Granitic Complex|64632|6|Mentioned|p201 Fig.1|||Pilbara Craton||||||
74678|Yule Granitic Complex|65827|6|Mentioned|p16, p43|Paleoarchean||Has a central c.3240 Ma intrusion; dyke swarm in this complex dated at 755 +/- 3 Ma (SHRIMP U-Pb zircon).
||||||
74678|Yule Granitic Complex|66118|5|Briefly described|p150, p157|||Ages: Fig. 2; Smithies and Farrell, 2000; Smithies, 2003. [Not a stratigrapic term].|c.3420Ma tonalites, c.3068 & 2940-2930Ma granites||Cockeraga Leucogranite|Encloses Cheearra greenstone belt.|Variety of different granitic rocks, including tonalites and granites.|26-MAY-20
74678|Yule Granitic Complex|66217|5|Briefly described|p24, p56.||||||Includes Callina Supersuite intrusions.|Is intruded by Mundine Well Dolerite Suite and Round Hummock Dolerite Suite.||
74678|Yule Granitic Complex|67197|6|Mentioned|p3|||East Pilbara Terrane.||||||
74678|Yule Granitic Complex|67270|6|Mentioned|p3|Archean|Archean|||||||
74678|Yule Granitic Complex|68035|6|Mentioned|284 Fig 1|Archean|Archean|||||||
74678|Yule Granitic Complex|70022|6|Mentioned|p114|||Pilbara Craton.||||||
33198|Yule Granitoid Complex|23416|5|Briefly described|Map Legend|Archean|Archean|Pilbara Craton||||||07-NOV-08
33198|Yule Granitoid Complex|23755|4|Described|p54|Archean|Archean|Age:  c.3240 Ma (SHRIMP U-Pb)||||||07-NOV-08
33198|Yule Granitoid Complex|23783|5|Briefly described|p9 Fig. 4, p18|||||||||
33198|Yule Granitoid Complex|23813|5|Briefly described|p101|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|23895|5|Briefly described|p884 Fig.1|||||||||
33198|Yule Granitoid Complex|23936|5|Briefly described|p3, Fig.4|Archean|Archean|Age: ca. 3450 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|24025|5|Briefly described|p11 Tb. 2|Archean|Archean|Age: 3470-2927Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|24110|5|Briefly described|Plate 1|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33198|Yule Granitoid Complex|24166|5|Briefly described|p18|Archean|Archean|||||||07-NOV-08
33198|Yule Granitoid Complex|24184|4|Described|p703|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.2935Ma||||||07-NOV-08
33198|Yule Granitoid Complex|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Geological Province: Mallina basin||||||07-NOV-08
33198|Yule Granitoid Complex|24190|5|Briefly described|p820 Fig.1|Archean|Archean|||||||07-NOV-08
33198|Yule Granitoid Complex|24193|5|Briefly described|p889 Fig.1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|24531|4|Described|p23|Archean|Archean|Age: c.3420Ma.  See also p8-9 Fig. 3.||||||07-NOV-08
33198|Yule Granitoid Complex|24532|5|Briefly described|Map legend|Archean|Archean|Age: c.2933-2927Ma.||||||07-NOV-08
33198|Yule Granitoid Complex|24533|5|Briefly described|p1, p7|Archean|Archean|Outcrops of gneissic monzogranite to granodiorite in the East Pilbara Granite-Greenstone Terrane. Unconformably overlain by the Fortescue Group. Age: c.3420Ma.||||||07-NOV-08
33198|Yule Granitoid Complex|24534|5|Briefly described|Map legend|Archean|Archean|Age: 2935Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|24554|4|Described|p1, p8|Archean|Archean|Age: c. 3420-2927 Ma. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
33198|Yule Granitoid Complex|44150|5|Briefly described|p130-131 Fig.2-130,p135,p142-144 Tb.2-21|||See also p149 Fig.2-137, p152, p153 Fig.2-140, p155 Fig.2-142. Covers 6000 sq km.|||Includes Numbana Granite; Nardoopiquithanna, Kangan, Pincunah, Abydos, Woodstock, Coorong Creek Adamellites; Mount Gratwick, Tambourah Granodiorites.||Monzogranites, granodiorites, granite, gneiss, greenstones.|
33198|Yule Granitoid Complex|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
33198|Yule Granitoid Complex|50146|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|50370|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
33198|Yule Granitoid Complex|50379|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
33198|Yule Granitoid Complex|50423|6|Mentioned|p216||Archean|||||||07-NOV-08
33198|Yule Granitoid Complex|50427|6|Mentioned|p174|Archean|Archean|||||||07-NOV-08
33198|Yule Granitoid Complex|63372|5|Briefly described|Map Legend|Archean|Archean|Granitic rock undivided. Geological Province: East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
33198|Yule Granitoid Complex|65455|6|Mentioned|p5|Archean|Archean|Pilbara Craton.||||||09-MAY-12
33198|Yule Granitoid Complex|66882|5|Briefly described|p118|Neoarchean|Paleoarchean|Pilbara Craton. A possible source for Mesoarchean zircons in Cook Gap Schist (Gawler Craton).|3166 +/- 5 Ma (Nelson, 2000).||||Tonalite.|
33198|Yule Granitoid Complex|67721|6|Mentioned|p37|||Contains a c. 3165 tonalite.||||||
33198|Yule Granitoid Complex|69300|5|Briefly described|map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane. Isotopic age: shown on legend as 3430-2850 Ma; also of Kenny (2000).|3428+/-6 Ma (isotopic age, Nelson 2002)||||undivided tonalite to monzogranite; metamorphosed|
39781|Yule granitoid complex|24193|5|Briefly described|p874 Fig.1|Archean|Archean|Geological Province: Pilbara Craton. Informal name - see Yule Granitoid Complex.||||||07-NOV-08
39281|Yulleroo Gas Sands|24246|5|Briefly described|p12, 13|||Informal. Geological Province: Canning Basin.||||||
39282|Yulleroo gas sands|24246|6|Mentioned|p13|||Informal. Geological Province: Canning Basin.||||||
31424|Zebra Hill Dyke|43597|5|Briefly described|p716|||||||||
73583|Zebra Hill Suite|63441|5|Briefly described|p13 tb. 2, p38|Archean|Archean|Unconformably overlain by Hardey Formation (Fortescue Group). Geological province: Pilbara Craton. East-west striking gabbro and pyroxene dykes on PINDERI HILLS, cutting the Munni Munni layered intrusion (of Radley Suite).||||||07-FEB-11
73583|Zebra Hill Suite|64174|5|Briefly described|Map legend|Archean|Archean|Dolerite and pyroxenite dyke.||||||07-NOV-08
41956|Zebra rock|34230|4|Described|p67-68|Proterozoic|Proterozoic|A striking red and white banded rock, the formation of which is not easily explained.  Occurs as sparsely distributed elongate lenses in the upper part of the Ranford Formation.||||||28-OCT-04
82278|Zuytdorp Limestone""|69558|6|Mentioned|p103|||Of Hearty and O'Leary (2008). Invalid name apparently for part of Tamala Limestone, in Womerangee Hill area.||||||
36004|actinolite 36004|44443|6|Mentioned|Map legend||Archean|Actinolite/tremolite/hornblende - chlorite - plagioclase rock; probably metamorphosed magnesia - rich basalt.||||||07-NOV-08
33093|adamellite 33093|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Even grained granitic rocks - fine to medium-grained granodiorite, adamellite and granite, often partially recrystallized.||||||
33095|adamellite 33095|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Fine to medium-grained adamellite and granite with scattered microcline megacrysts.||||||
33102|adamellite 33102|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33102|adamellite 33102|44443|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Hornblende-adamellite/quartz-monzonite.||||||07-NOV-08
35964|adamellite 35964|44443|5|Briefly described|map legend|Archean|Archean|Biotite adamellite and biotite granodiorite, well foliated, commonly gneissic and migmatitic.||||||07-NOV-08
35795|amphibolite 35795|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Hornblende-plagioclase (-garnet-actinolite-clinopyroxene) amphibolite; fine and medium-grained. Morrissey Metamorphic Suite.||||||07-NOV-08
35795|amphibolite 35795|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Hornblende-plagioclase amphibolite. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35795|amphibolite 35795|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic| Shown as -Pnm  Amphibolititc gneiss.||||||07-NOV-08
35795|amphibolite 35795|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Hornblende-plagioclase (-garnet-actinolite-clinopyroxene) amphibolite; fine and medium-grained. Of Morrissey Metamorphic Suite.||||||
35795|amphibolite 35795|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Hornblende-plagioclase (-actinolite-epidote) amphibolite.  Part of Morrissey Metamorphic Suite.||||||07-NOV-08
35724|augen gneiss 35724|39794|6|Mentioned|Map legend||Proterozoic|Augen gneiss, coarse-grained with microcline augen, strong cataclastic foliation. Derived from porphyritic granite.||||||
35801|banded gneiss 35801|37024|6|Mentioned|Map legend|Archean|Archean|Quartz-feldspar-biotite (-garnet) gneiss, includes orthogneiss, with biotite rich and quartz-feldspar rich layers, includes large amounts of granitoid and pegmatoid rock, in some areas Anb grades into Am and A-Pnb into A-Pm units.||||||07-NOV-08
35801|banded gneiss 35801|40357|6|Mentioned|Map legend|Archean|Archean|Quartz-feldspar-biotite gneiss and migmatite, compositionally banded.||||||07-NOV-08
35801|banded gneiss 35801|40935|6|Mentioned|Map legend|Archean|Archean|Banded, microcline-plagioclase-quartz-biotite gneiss, coarse to fine-grained; migmatitic in part.||||||07-NOV-08
35801|banded gneiss 35801|43255|5|Briefly described|map legend|Archean|Archean| Banded, microcline-plagioclase-quartz-biotite gneiss; coarse to fine-grained, migmatitic in part.||||||07-NOV-08
35896|banded granulite 35896|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Granulite - well banded, contains microcline.||||||
35896|banded granulite 35896|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Symbol -Pn on this sheet. Granulite - well banded, dominantly acid composition. Charnockites present. Show flaser structures, migmatisation and complex, repeated folding. Polymetamorphic.||||||
35637|basal Triassic sandstone|23279|6|Mentioned|p20|||(Hall, 1989). Present name: Dongara Sandstone.||||||
35802|biotite adamellite 35802|37024|6|Mentioned|Map legend|Archean|Archean|Biotite adamellite and granite, medium to coarse-grained.||||||07-NOV-08
35802|biotite adamellite 35802|40357|6|Mentioned|Map legend|Archean|Archean|Biotite granite, adamellite, granodiorite and tonalite, even-grained.||||||07-NOV-08
35802|biotite adamellite 35802|43255|5|Briefly described|map legend|Archean|Archean| Biotite adamellite; coarse to medium-grained.||||||07-NOV-08
35976|carbonate-talc rock 35976|44443|5|Briefly described|map legend|Archean|Archean|Carbonate-talc rock. Primary mineralogy generally indeterminate.||||||07-NOV-08
35968|chert 35968|44443|5|Briefly described|map legend|Archean|Archean|Chert (not subdivided).||||||07-NOV-08
35725|dioritic rock 35725|39794|6|Mentioned|Map legend||Archean|Dioritic rocks, range from monzonite to diorite. Small intrusions only.||||||07-NOV-08
35967|dolerite dyke 35967|44443|5|Briefly described|map legend|Archean|Archean|Dolerite dyke or sill.||||||07-NOV-08
35811|dolomite 35811|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed dolomite and siliceous or feldspathic dolomite.||||||07-NOV-08
35811|dolomite 35811|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Dolomite, locally stromatolitic.||||||07-NOV-08
36048|dolomite 36048|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Dark grey dolomite and calcarenite.||||||
33089|felsite 33089|30962|6|Mentioned|Map legend|Proterozoic|Proterozoic|Part of Mount Ragged Beds.||||||
35711|foliated granitoids 35711|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
35711|foliated granitoids 35711|30975|6|Mentioned|Map legend|Archean|Archean|Strongly foliated granitic rocks; granodiorite to tonalite.||||||07-NOV-08
35962|gabbro 35962|44443|5|Briefly described|map legend|Archean|Archean|Gabbro dyke or sill.||||||07-NOV-08
31867|gneiss 31867|43848|5|Briefly described|Map Legend||Proterozoic|||||||
33052|gneiss 33052|30954|6|Mentioned|Map legend||Proterozoic|Garnet-biotite-quartz-feldspar gneiss containing feldspar augen.||||||
33073|gneiss 33073|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
33074|gneiss 33074|30961|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
33083|gneiss 33083|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33084|gneiss 33084|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33098|gneiss 33098|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Augen gneiss; developed from -Pgp (stratno 33099)||||||
33100|gneiss 33100|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Augen gneiss; coarse-grained with microcline augen.||||||
33101|gneiss 33101|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Gneiss; granoblastic granite, adamellite with streaks of granoblastic minerals (biotite, hornblende or pyroxene) or magnetite, garnet common; includes mior layered or granofelsic rocks.||||||
35715|gneiss 35715|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
35728|gneiss 35728|39794|6|Mentioned|Map legend||Archean|Quartz-feldspar-biotite-garnet gneiss.||||||07-NOV-08
35729|gneiss 35729|39794|6|Mentioned|Map legend||Proterozoic|Quartz-feldspar-biotite(-garnet) gneiss.||||||
35729|gneiss 35729|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-feldspar-biotite(-garnet-hypersthene) gneiss; compositionally layered gneiss with subordinate -Pns 33101 and granofels; includes amphibolite and mafic granulite layers; granoblastic fabric.||||||
35772|gneiss 35772|40357|5|Briefly described|Map legend|Archean|Archean|Adamellite and granodiorite gneiss with strong gneissic foliationand lineation, commonly compositional banded, includes augen gneiss.||||||07-NOV-08
35796|gneiss 35796|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Actinolite-tremolite-quartz-feldspar-clinopyroxene-epidote-sphene compositionally layered assemblages; calc-silicate gneiss and granofels. Morrissey Metamorphic Suite.||||||07-NOV-08
35796|gneiss 35796|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Tremolite-actinolite-plagioclase-quartz-microcline-clinopyroxene-epidote-sphene-hornblende-garnet compositionally layered assemblages; calc-silicate gneiss. Of Morrissey Metamorphic Suite.||||||
35796|gneiss 35796|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Tremolite-actinolite-quartz-plagioclase-epidote (-hornblende-clinopyroxene-garnet) compositionally layered assemblages; calc-silicate gneiss.  In Morrissey Metamorphic Suite.||||||07-NOV-08
35907|gneiss 35907|35252|6|Mentioned|Map legend|Proterozoic|Proterozoic|Banded quartz-magnetite-amphibole gneiss.||||||
35934|gneiss 35934|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|Overprinted hornblende-plagioclase (-quartz-diopsite) gneiss and amphibolite||||||
35935|gneiss 35935|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|Overprinted garnet-bearing hornblende-plagioclase (-quartz-diopsite) gneiss and amphibolite.||||||
35936|gneiss 35936|35252|6|Mentioned|Map legend|Proterozoic|Proterozoic|banded quartz-feldspar-garnet-epidote-amphibole gneiss; quartz-feldspar-garnet-staurolite-chlorite schist; paragneiss.||||||
35936|gneiss 35936|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|Retrograded quartz-feldspar-epidote-garnet (-mica-tremolite) paragneiss.||||||
36010|gneiss 36010|37016|6|Mentioned|Map legend||Proterozoic|Gneiss, mainly quartzo - feldspathic. Not subdivided.||||||
36030|gneiss 36030|30943|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Coarse porphyritic granite and medium-grained granite.||||||
33067|gneiss and migmatite 33067|30975|6|Mentioned|Map legend|Proterozoic|Proterozoic|Banded quartz-feldspar-biotite-garnet gneiss and migmatite.||||||
33071|gneissic adamellite 33071|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
31334|granite 31334|43592|5|Briefly described|map legend|Precambrian|Precambrian|Granite gneiss: mainly potassic, strongly to weakly foliated usually concordant; always present between basic granulite and coarse-grained granulite.||||||
33053|granite 33053|30954|6|Mentioned|Map legend|Proterozoic|Archean|Granite and gneiss - undifferentiated.||||||07-NOV-08
33054|granite 33054|30954|6|Mentioned|Map legend|Proterozoic||Mixed granites.||||||
33055|granite 33055|30954|6|Mentioned|Map legend|Proterozoic||Granite with potassium feldspar phenocrysts.||||||
33063|granite 33063|30954|6|Mentioned|Map legend|Proterozoic||Equigranular leucocratic granite||||||
33070|granite 33070|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
33076|granite 33076|30961|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
33080|granite 33080|30959|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of Mount Andrew Migmatites.||||||
33082|granite 33082|30959|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of Mount Andrew Migmatites.||||||
33085|granite 33085|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33090|granite 33090|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33091|granite 33091|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33094|granite 33094|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|mixed granitic rocks, chiefly interdeveloped even-grained and porphyritic granite||||||
33099|granite 33099|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Porphyritic biotite granite and adamellite.||||||
33108|granite 33108|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
35710|granite 35710|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
35710|granite 35710|31093|6|Mentioned|p13|||||||||
35714|granite 35714|30959|6|Mentioned|Map legend|Archean|Archean|Biotite granite - equigranular.||||||07-NOV-08
35714|granite 35714|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
35714|granite 35714|30975|6|Mentioned|Map legend|Archean|Archean|Granite to adamellite; fine to medium grained.||||||07-NOV-08
35808|granite 35808|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Weakly banded, coarse-grained biotite (-muscovite) tonalite to adamellite; commonly has stictolithic structure and biotite schlieren; transitional phase between migmatite and homogenous granitoid||||||07-NOV-08
35966|granite 35966|44443|5|Briefly described|map legend|Archean|Archean|Medium to coarse, even-grained granite and adamellite. Poorly foliated.||||||07-NOV-08
36033|granite 36033|30943|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit for Proterozoic Granites GIS. Desc: Fine grained granite with very large, scattered, euhedral and rounded feldspar phenocrysts. Includes aplitic granite and mixed granites with bands of and rafts of -Pbo.||||||
36038|granite 36038|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Undifferentiated granitic rocks.||||||
36039|granite 36039|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Granite.||||||
36040|granite 36040|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Granite.||||||
33069|granite and gneiss 33069|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
33066|granitic gneiss 33066|30975|6|Mentioned|Map legend|Proterozoic|Proterozoic|Granitic gneiss; strongly foliated adamellite to granodiorite; garnetiferous.||||||
33109|granitic gneiss 33109|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Granitic gneiss, coarse-grained orthogneiss.||||||
33109|granitic gneiss 33109|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Granitic gneiss; fine to medium-grained with subordinate megacrystic varieties; weak foliation; granoblastic texture||||||
35726|granitic gneiss 35726|39794|6|Mentioned|Map legend||Archean|Granitic gneiss, coarse-grained orthogneiss, commonly with braided biotite foliation, includes local augen gneiss and migmatite.||||||07-NOV-08
35780|granitic gneiss 35780|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Muscovite-biotite-granodioritic, adamellitic paragneiss; metamorphosed arkose; retrograde varieties are phyllonitic, includes some mica schist.||||||07-NOV-08
35780|granitic gneiss 35780|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Granitic gneiss.||||||07-NOV-08
36009|granitic gneiss 36009|37016|6|Mentioned|Map legend||Proterozoic|Granitic gneiss.||||||
36027|granitic gneiss 36027|30946|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Granitic gneiss, closely related to -Psa and -Psf.||||||
36037|granitic gneiss 36037|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Granitic gneiss.||||||
33086|granitic rocks 33086|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
31880|granitoid 31880|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|of Sally Downs supersuite, Bow River batholith.||||||
31871|granodiorite 31871|43849|5|Briefly described|Map Legend||Proterozoic|||||||
33081|granodiorite 33081|30959|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of Mount Andrew Migmatites.||||||
33092|granodiorite 33092|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Coarse, even-grained granodiorite, adamellite and granite.||||||
35767|granofels 35767|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sericitized and chloritized muscovite, quartz andalusite (-biotite chloritoid- staurolite-?cordierite) granofels.||||||07-NOV-08
35767|granofels 35767|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite-quartz schist with deformed pebbles of vein quartz, metaconglomerate.||||||07-NOV-08
35767|granofels 35767|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-biotite-sillimanite (-muscovite-cordierite-plagioclase-tourmaline-staurolite-andalusite) schist and granofels. Of Morrissey Metamorphic Suite.||||||
35766|granofels and schist 35766|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Chlorite-amphibolite-calcite-dolomite (-quartz) granofels and schist.||||||07-NOV-08
35766|granofels and schist 35766|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Chlorite-muscovite-quartz-schist.||||||07-NOV-08
36035|granophyre 36035|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Granophyre closely associated with Skirmish Hill Volcanic Association.||||||
31333|granulite 31333|43592|5|Briefly described|map legend|Precambrian|Precambrian|Medium-grained granulite: foliated and banded; locally garnetiferous.||||||
35862|granulite 35862|43592|5|Briefly described|map legend|Precambrian|Precambrian|Coarse-grained granulite: banded and foliated, white with dark banding.||||||
35863|granulite 35863|43592|5|Briefly described|map legend|Precambrian|Precambrian|Basic granulite: dark, banded amphibole and amphibole-pyroxene rocks occurring in thin bands; often ias xenoliths in granite gneiss.||||||
35897|granulite 35897|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Granulite - Poorly banded, contains orthoclase.||||||
35965|greenstone 35965|44443|5|Briefly described|map legend|Archean|Archean|Greenstone xenoliths and Agm (biotite adamellite and biotite granodiorite, well foliated, commonly gneissic and migmatitic) in aproximately equal proportions.||||||07-NOV-08
67827|indjana Limestone|24371|5|Briefly described|p216 Fig.9|Famennian|Frasnian|Informal name. Unconformably overlies Napier Formation. Overlain by Nullara Formation. Geological province: Canning Basin.||||||24-FEB-05
33072|leucocratic granite 33072|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
35727|mafic hornfels & amphibolite 35727|39794|6|Mentioned|Map legend||Archean|Fine to medium grained leucocratic granulite, with perthitic feldspar and hypersthene.||||||07-NOV-08
35774|mafic rocks 35774|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Mafic rocks.||||||07-NOV-08
35797|marble 35797|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Calcite and/or dolomite-tremolite-actinolite (chlorite-humite-quartz) marble. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35797|marble 35797|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Dolomite-Mg-chlorite-tremolite marble. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35797|marble 35797|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Shown as -Pnd  Calcareous gneiss with bands of marble or recrystallized dolomite.||||||07-NOV-08
35797|marble 35797|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Calcite and or dolomite (-tremolite-actinolite-chlorite-quartz-sepentine-? humite-phlogopite) marble. Morrissey Metamorphic Group.||||||
35797|marble 35797|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Dolomite- calcite (-tremolite-actinolite-chlorite-quartz-serpentine-phlogopite) marble.  Part of Morrissey Metamorphic Suite.||||||07-NOV-08
35768|microgneiss and schist 35768|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-feldspar-biotite-muscovite microgneiss and schist; metamorphosed greywacke.||||||07-NOV-08
35768|microgneiss and schist 35768|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Biotite-muscovite (-garnet)  - granodioritic microgneiss, with intercalated pelitic schist.||||||07-NOV-08
35768|microgneiss and schist 35768|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-plagioclase-microcline-biotite-muscovite (-garnet) microgneiss and schist; metamorphosed greywacke and shale||||||
35756|migmatite  35756|37024|6|Mentioned|Map legend|Archean|Archean|Migmatite, palaeosome of quartz-feldspar-biotite gneiss, neosome of granite, mainly stromatic structure.||||||07-NOV-08
33068|migmatite 33068|30945|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
33077|migmatite 33077|30961|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
33078|migmatite 33078|30970|6|Mentioned|Map legend|Proterozoic|Archean|||||||07-NOV-08
33079|migmatite 33079|30959|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of Mount Andrew Migmatites.||||||
33087|migmatite 33087|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33088|migmatite 33088|30962|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
33096|migmatite 33096|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Migmatite - nebulitic or with strongly contorted banding. Palaeosome often a streaked-out augen gneiss.||||||
33096|migmatite 33096|39795|6|Mentioned|Map legend|Proterozoic|Proterozoic|Migmatite; granoblastic or gneissic palaoesome (-Pnb , -Pna 33100) and allotriomorphic granular neosome of -Pgp 33099||||||
35713|migmatite 35713|30959|6|Mentioned|Map legend|Archean|Archean|Migmatite; marginal between Archaean formations and granite.||||||07-NOV-08
35713|migmatite 35713|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
35798|migmatite 35798|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Migmatite with palaeosome: calc-silicate gneiss, amphibolite, marble, pelitic schist + quartzo-feldspathic gneiss; neosome: muscovite biotite granite + adamellite. Of Morrissey Metamorphic Suite||||||07-NOV-08
35803|migmatite 35803|40935|6|Mentioned|Map legend|Proterozoic|Archean|Migmatite with banded microcline-plagioclase-quartz-biotite gneiss palaeosome, and a neosome of anatectic biotite (-muscovite) adamellite and granite.||||||07-NOV-08
35803|migmatite 35803|43255|5|Briefly described|map legend|Archean|Archean|Migmatite with banded microcline-plagioclase-quartz-biotite gneiss and 30 percent or more anatectic, biotite adamellite and granite.  Archaean gneissic terrain which has undergone Proterozoic anatexis.||||||07-NOV-08
35804|migmatite 35804|40935|6|Mentioned|Map legend|Proterozoic|Archean|Migmatite with fine-grained biotite tonalite, granodiorite or quartz-diorite gneiss palaeosome and a neosome of anatectic biotite granodiorite.||||||07-NOV-08
35804|migmatite 35804|43255|5|Briefly described|map legend|Archean|Archean|Migmatite with fine-grained, banded, biotite tonalite or granodiorite gneiss, varying amphibolite and 30% or more anatectic biotite granodiorite.  Archaean gneissic terrain which has undergone Proterozoic anatexis.||||||07-NOV-08
35805|migmatite 35805|40935|6|Mentioned|Map legend|Proterozoic|Archean|Pelitic and mafic granofels with migmatitic quartzo-feldspathic gneiss.||||||07-NOV-08
35805|migmatite 35805|43255|5|Briefly described|map legend|Archean|Archean|Pelitic and mafic granofels with migmatitic, quartzofeldspathic gneiss.  Archaean gneissic terrain which has undergone Proterozoic anatexis.||||||07-NOV-08
35807|migmatite 35807|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite with a dark phase of paragneiss, schist, biotite schlieren, and minor calc-silicate gneiss and amphibolite;and a light phase of  biotite (-muscovite tourmaline) granitoid and pegmatoid. Morrissey Metamorphic Suite.||||||07-NOV-08
35807|migmatite 35807|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Paragneiss migmatite. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35807|migmatite 35807|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Migmatite with a palaeosome of mainly paragneiss also minor schist, calc-silicate gneiss and amphibolite, and a neosome of biotite-muscovite adamellite, granodiorite and pegmatite. Of Morrissey Metamorphic Suite.||||||
35807|migmatite 35807|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Migmatite with a palaeosome of paragneiss and schist  and a neosome of biotite (-muscovite) granitoid and pegmatoid.||||||07-NOV-08
35898|migmatite 35898|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Migmatite of granulite and granititc gneiss||||||
35898|migmatite 35898|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Symbol -Pgm on this sheet. Migmatites and granite with abundant enclaves.||||||
35806|migmatite and schist 35806|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite with a dark phase of schist, muscovite, biotite schlieren, and minor paragneiss;and a light phase of  muscovite (-biotite tourmaline) adamellite, granite and pegmatite. Morrissey Metamorphic Suite.||||||07-NOV-08
35806|migmatite and schist 35806|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Migmatite with a palaeosome of pelitic schist with minor paragneiss, calc-silicate gneiss, marble and amphibolite, and a neosome of muscovite-biotite-tourmaline adamellite, granite and pegmatite. Of Morrissey Metamorphic Suite.||||||
35806|migmatite and schist 35806|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Migmatite with palaeosome: mainly pelitic schist, also minor paragneiss, calc-silicate gneiss + amphibolite; neosome: muscovite(-biotite) adamellite, granite + pegmatite; commonly has tourmaline.||||||07-NOV-08
35753|muscovite schist 35753|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Fine to coarse-grained, quartz-muscovite-chlorite (-biotite)-epidote-sericite schist; metamorphosed wacke and pelite.||||||07-NOV-08
35753|muscovite schist 35753|35639|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite schist, quartz-muscovite schist.||||||07-NOV-08
40059|niobium tuff|24173|5|Briefly described|p17|||Informal reference to base of Butchers Gully Member. Of the Butchers Gully Member. Max Thickness: 35m. Hosts the Brockman deposit. Age: 1870Ma (zircon dating by Taylor et al, 1995a). See also "Niobium tuff" and "niobium tuff".||||||06-APR-05
40065|niobium tuff""|24173|5|Briefly described|p9 Tb.1|||Informal name. See also niobium tuff and "Niobium tuff". Overlain by Butchers Gully Member, of which it is a part. Highly strained fluorite bearing fine-grained rock. Age: 1868 +/- 3Ma is age of volcanic detritus within this rock||||||06-APR-05
40065|niobium tuff""|50542|5|Briefly described|p105|||Informal name: see Niobium Tuff. Vertical or steeply dipping trachytic ash-flow tuff. Width: 5-35m. Strike length of 3.5km. Geological Province: Halls Creek Orogen.||||||07-FEB-11
39183|older"" Ascot Formation|23768|5|Briefly described|p27, p181|||Informal name - see Ascot Formation. Geological Province: Perth Basin.||||||
31865|orthogneiss  31865|43848|5|Briefly described|Map Legend||Proterozoic|||||||
31868|orthogneiss 31868|43848|5|Briefly described|Map Legend||Proterozoic|On Rudall: orthogneiss derived from porphyritic biotite granite to monzogranite;generally contains..||||||
31868|orthogneiss 31868|43849|5|Briefly described|Map Legend||Proterozoic|||||||
31869|orthogneiss 31869|43849|5|Briefly described|Map Legend||Proterozoic|||||||
31870|orthogneiss 31870|43849|5|Briefly described|Map Legend||Proterozoic|||||||
31903|orthogneiss 31903|43848|5|Briefly described|Map Legend||Proterozoic|||||||
33097|orthogneiss 33097|39794|6|Mentioned|Map legend|Proterozoic|Proterozoic|Granitic gneiss, intensely deformed othrogneiss with conjugate folds common.||||||
35757|paragneiss 35757|37024|6|Mentioned|Map legend|Archean|Archean|Banded quartz-feldspar(-biotite-muscovite-garnet-amphibolite) rock, quartz-rich in places, mainly paragneiss.||||||07-NOV-08
35799|paragneiss 35799|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-biotite-muscovite-feldspar (-garnet) schist and paragneiss. Morrissey Metamorphic Suite.||||||07-NOV-08
35799|paragneiss 35799|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-biotite-muscovite-feldspar (-garnet) schist and paragneiss; medium to coarse-grained. Of Morrissey Metamorphic Suite.||||||
35799|paragneiss 35799|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartz-feldspar-biotite-muscovite paragneiss + schist with interfoliated quartz-biotite-muscovite- garnet(-sillimanite) schist + calc-silicate gneiss; muscovite granitoid + pegmatoid phases,migmatite in part. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35769|paragneiss and schist 35769|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-microcline-oligoclase-biotite-muscovite paragneiss and schist; medium to coarse-grained; metamorphosed arkose and feldspathic arenite.||||||07-NOV-08
35769|paragneiss and schist 35769|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-microcline-oligoclase-biotite-muscovite (-garnet) paragneiss and schist; medium to coarse-grained, metamorphosed arkose and feldspathic arenite. Morrissey Metamorphic Suite.||||||
31866|pegmatite 31866|43848|5|Briefly described|Map Legend||Proterozoic|||||||
35775|pelitic schist 35775|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Phyllite.||||||07-NOV-08
35775|pelitic schist 35775|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Pelitic schist.||||||07-NOV-08
35987|peridotite 35987|39424|6|Mentioned|Map legend|Archean|Archean|Peridotite and dunite. Light green and medium to coarse-grained. Partly serpentinized.||||||07-NOV-08
35987|peridotite 35987|44443|5|Briefly described|map legend|Archean|Archean|Peridotite.||||||07-NOV-08
35770|phyllite and schist 35770|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Sericite-chlorite-quartz-magnetite phyllite and fine-grained schist||||||07-NOV-08
35770|phyllite and schist 35770|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Sericite-chlorite-quartz-magnetite-tourmaline phyllite and fine-grained schist. Morrissey Metamorphic Suite.||||||
35963|porphyritic adamellite 35963|44443|5|Briefly described|map legend|Archean|Archean|Medium to coarse-grained, foliated porphyritic biotite adamellite; minor porphyritic granodiorite.||||||07-NOV-08
36036|porphyritic granite 36036|30942|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Porphyritic granite.||||||
36032|porphyritic microgranite 36032|30943|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit for Proterozoic Granites GIS. Desc: Porphyritic microgranite with very large feldspar laths; foliated.||||||
33104|porphyry dyke 33104|44443|5|Briefly described|map legend|Proterozoic|Proterozoic|Hornblende porphyry dyke, related to -Pgh.||||||
35777|quartz arenite 35777|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated, coarse-grained arkose,feldspathic arenite and granule comglomerate; metamorphosed at low grade.||||||07-NOV-08
35777|quartz arenite 35777|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz arenite with minor rudite.||||||07-NOV-08
35778|quartz wacke 35778|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quatz wacke.||||||07-NOV-08
35800|quartzite 35800|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Foliated quartzite and micaceous quartzite. Morrissey Metamorphic Suite.||||||07-NOV-08
35800|quartzite 35800|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Fine-grained, granoblastic-textured quartzite. Of Morrissey Metamorphic Suite.||||||07-NOV-08
35800|quartzite 35800|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated quartzite and micaceous quartzite.  Part of Morrissey Metamorphic Suite.||||||07-NOV-08
35908|quartzite 35908|35252|6|Mentioned|Map legend|Proterozoic|Proterozoic|Foliated quartzite.||||||
35908|quartzite 35908|35387|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartzite, foliated.||||||
36050|quartzite 36050|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Fine to medium quartzite and quartz sandstone, locally pyritiferous.||||||
35776|quartzite bands 35776|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzite bands in gneiss.||||||07-NOV-08
36031|rapakivi granite 36031|30943|6|Mentioned|Map legend||Mesoproterozoic|Unnamed unit for Proterozoic Granites GIS. Desc: Rapakivi granite - granite with large ovoids of potash feldspar and quartz granules. In places sheared, serific with streched ovoids and granules.||||||
33075|rocks 33075|30961|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
35779|rudite 35779|37016|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Rudite.||||||07-NOV-08
35937|sandstone 35937|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Fine to medium quartzite and quartz sandstone, massive to well-bedded, locally flaggy||||||
35938|sandstone 35938|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Transition beds of intercalated sandstone, siltstone and shale.||||||
36047|sandstone 36047|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Fine to medium quartzite and quartz sandstone.||||||
36049|sandstone 36049|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Transition beds of intercalated sandstone and shale.||||||
35754|schist 35754|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-muscovite-biotite (-sericite-chlorite-andalusite-garnet-tourmaline) schist, includes prograde and retrograde assemblages.||||||07-NOV-08
35754|schist 35754|35639|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite schist, quartz muscovite schist (metamorphosed wacke and shale).||||||07-NOV-08
35754|schist 35754|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite-quartz schist or phyllite, contains minor hematite.||||||07-NOV-08
35754|schist 35754|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-muscovite-tourmaline (-biotite-chlorite-sericite-epidote-andalusite-magnetite-garnet-chloritoid) schist, fine to coarse-grained. some phases are retrogressive. Of Morrissey Metamorphic Suite.||||||
35754|schist 35754|43255|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartz-sericite-muscovite-chlorite (-magnetite-tourmaline-biotite-chloritoid) schist, retrograde in part.||||||07-NOV-08
35755|schist 35755|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed, schistose conglomerate, with interlayered pelitic schist and quartzite. Of Morrissey Metamorphic Group.||||||07-NOV-08
35755|schist 35755|37024|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-graphite schist.||||||07-NOV-08
35771|schist 35771|23310|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-muscovite-biotite-garnet (-staurolite-andalusite-chlorite-sillimanite-cordierite) schist.||||||07-NOV-08
35771|schist 35771|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Quartz-biotite-muscovite-garnet-tourmaline (-staurolite-andalusite-chlorite-sillimanite-cordierite) schist, medium and coarse-grained. Of Morrissey Metamorphic Suite.||||||
35781|schist 35781|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Fine-grained quartz-hornblende-quartz-epidote-magnetite- (biotite-chlorite) schist||||||07-NOV-08
35781|schist 35781|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|Hornblende-quartz-epidote-magnetite (-biotite-chlorite) schist. Of Morrissey Metamorphic Group.||||||
35782|schist 35782|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Dark-grey, fine-grained, quartz-biotite-muscovite-garnet schist||||||07-NOV-08
35783|schist 35783|23311|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Medium to coarse-grained, quartz-muscovite-biotite(-chlorite) schist||||||07-NOV-08
35988|schist 35988|44443|5|Briefly described|map legend|Archean|Archean|Amphibole-plagioclase schist.||||||07-NOV-08
36005|schist 36005|44229|5|Briefly described|Map Legend||Archean|Hornblende - plagioclase schist; after dolerite intrusions; restricted to Duffer Formation.||||||07-NOV-08
36011|schist 36011|37016|6|Mentioned|Map legend||Proterozoic|Quartz chlorite-muscovite schist.||||||
35973|sediments 35973|44443|5|Briefly described|map legend|Archean|Archean|Clastic sedimentary rocks (not subdivided).||||||07-NOV-08
35975|serpentinite 35975|44443|5|Briefly described|map legend|Archean|Archean|Serpentinite. Primary mineralogy uncertain||||||07-NOV-08
30713|sheared granitoid 30713|42710|6|Mentioned|map legend|Proterozoic|Proterozoic|||||||
30713|sheared granitoid 30713|43281|5|Briefly described|map legend|Proterozoic|Proterozoic|Sheared granitoid rocks.||||||
35712|ultramafic 35712|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
35712|ultramafic 35712|30975|6|Mentioned|Map legend|Archean|Archean|Ultramafic rock; deeply weathered and silicified.||||||07-NOV-08
35773|ultramafic rock 35773|37024|6|Mentioned|Map legend|Archean|Archean|Undifferentiated, medium-grained ultramafic rock.||||||07-NOV-08
35773|ultramafic rock 35773|40357|5|Briefly described|Map legend|Archean|Archean|Undivided ultramafic rock.||||||07-NOV-08
35773|ultramafic rock 35773|40935|6|Mentioned|Map legend|Archean|Archean|Tremolite-actinolite-chlorite-sepentine-talc-carbonate assemblages; metamorphosed peridotite or pyroxenite.||||||07-NOV-08
35974|ultramafic rock 35974|44443|5|Briefly described|map legend|Archean|Archean|Ultramafic rock (not subdivided).||||||07-NOV-08
35640|upper Yarragadee|23279|6|Mentioned|p30|||Former name for Parmelia Formation.||||||
35638|upper sandstone member|23279|6|Mentioned|p21|||Member of Dongara Sandstone.||||||
38622|younger granite""|23784|6|Mentioned|p53|||Informal - no name.||||||
39184|younger"" Ascot Formation|23768|5|Briefly described|p27, p181|||Informal name - see Ascot Formation. See also "Younger" Ascot Formation. Geological Province: Perth Basin.||||||10-MAR-05
38608|younger"" granite suite|23784|5|Briefly described|p53|Archean|Archean|Age: 2880Ma.||||||07-NOV-08
69196|zebra gneiss|24542|5|Briefly described|p7|Proterozoic|Proterozoic|Not intended as a formal name. Banded hornblende-plagioclase rock. Of Leeuwin Complex.||||||
