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
3|81-Mile Vent Lamproite|41158|6|Mentioned|Table 33|||||||||
59|Abney Sandstone|13194|4|Described|p393 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: Abney Hill 15o44'S 128o45'E. 45-200m thick. Tidal and fluvial deposits.||||Overlies Kununurra Formation (conformably). Overlies Kellys Knob Sandstone (disconformably).  Overlain by Cecil Sandstone (conformably).|Red quartz and feldspathic sandstone; minor siltstone.|
59|Abney Sandstone|40792|6|Mentioned|Fig.5|||||||||
59|Abney Sandstone|40993|6|Mentioned|p4|||||||||
59|Abney Sandstone|41864|3|Fully described|p53|||||||||
59|Abney Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
59|Abney Sandstone|42030|5|Briefly described|p749|||||||||
59|Abney Sandstone|42175|5|Briefly described|Fig.2 P200|||||||||
59|Abney Sandstone|45038|14|Not recorded|p.23|||||||||
59|Abney Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
59|Abney Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
59|Abney Sandstone|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
59|Abney Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
155|Agnes Venture Slate|23926|5|Briefly described|p14 Fig. 3|Archean|Archean|Of Woolyeenyer Formation.    Geological Province: Yilgarn Craton.||||||07-NOV-08
155|Agnes Venture Slate|42195|5|Briefly described|p143|||||||||
155|Agnes Venture Slate|42353|5|Briefly described|Fig.23, Fig.59|||See also p18, Fig,11||||||24-AUG-22
4193|Ainslie Volcanics (WA)|23818|5|Briefly described|p45|Proterozoic|Proterozoic|Geological Province: Musgrave Block. Age: 1000 Ma.||||||18-APR-05
4193|Ainslie Volcanics (WA)|30388|6|Mentioned|p12|||Refers Sofoulis(1962) Lower part now Lilian Formation||||||
4193|Ainslie Volcanics (WA)|30390|6|Mentioned|p81|||||||||
4193|Ainslie Volcanics (WA)|31393|6|Mentioned|Pl.25|||M. Proterozoic. Chart only||||||
4193|Ainslie Volcanics (WA)|34537|6|Mentioned|p45|||||||||
187|Airlie Member|42598|3|Fully described|p90|Berriasian (Neocomian)||Technically invalid name. Airlie Volcanics, Qld has priority.||||||
213|Albany Granite|23818|6|Mentioned|p44|||Geological Province: Gawler Platform.||||||
213|Albany Granite|30387|6|Mentioned|p35|||Cause of large gravity low||||||
213|Albany Granite|30878|6|Mentioned|p51|||Precambrian. On Stratigraphic table||||||
213|Albany Granite|31393|6|Mentioned|Pl.25|||M. Proterozoic. Chart only||||||
213|Albany Granite|32586|6|Mentioned|p113|||||||||
213|Albany Granite|33468|6|Mentioned|p199|||1100my||||||
213|Albany Granite|34537|6|Mentioned|p44|||||||||
213|Albany Granite|39056|6|Mentioned|p570|||||||||
213|Albany Granite|64769|6|Mentioned|p34|Mesoproterozoic|Mesoproterozoic|Dimension stone name. Quarried from the Mount Melville area. WA. Grey, megacrystic granitoid.||||||
213|Albany Granite|65487|5|Briefly described|p56 Fig. 27|||Intruded into the Nornalup Zone during Stage I of the Albany-Fraser Orogen. Fig.27 shows age as c.1300 Ma.||||||
213|Albany Granite|68186|6|Mentioned|p8|||Nornalup Zone, Kepa Kurl Booya Province.||||||
213|Albany Granite|69252|6|Mentioned|p9|||Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.||||||
213|Albany Granite|71783|14|Not recorded|p83|||Age: 1,1000 m. y.; Igneous activity equated with granitic rocks at Archipelago of the Recherche region.||||||
271|Alinga Formation|12729|5|Briefly described|p.17||Cretaceous|||Winning Group||Overlies the Windalia Radiolarite, coeval with the Gearle Siltstone.|Greensand.|16-SEP-15
271|Alinga Formation|14228|6|Mentioned|p9|Cretaceous|Cretaceous|||Winning Group||Overlies Windalia Radiolarite. Equivalent to Gearle Siltstone. Overlain by Haycock Marl.|Glauconitic mudstone.|05-OCT-16
271|Alinga Formation|23572|4|Described|p12|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Underlying Unit: Windalia Sandstone Member.||||||04-MAY-05
271|Alinga Formation|23726|5|Briefly described|p26|||Overlying unit Toolonga Calcilutite. Underlying unit Windalia Radiolarite Geological Province: Carnarvon Basin.||||||
271|Alinga Formation|23815|4|Described|p297, 298|Turonian|Albian|Formerly known as "Alinga Beds" or "Alinga Greensands". Geological Province: Carnarvon Basin. Overlying unit: Toolonga Calcilutite (disconformable). Underlying unit: Windalia Radiolarite (conformable). Max. thickness: 15 m.||||||05-OCT-16
271|Alinga Formation|24094|5|Briefly described|p268, p275|||Overlain disconformably by Toolonga Calcilutite. Geological Province: Carnarvon Basin.||||||15-DEC-08
271|Alinga Formation|24160|5|Briefly described|p36|Cretaceous|Cretaceous|Southern Carnarvon Basin.||Winning Group||Conformably overlies Windalia Radiolarite; grades laterally into Gearle Siltstone.|Glauconitic siltstone and greensand.|
271|Alinga Formation|24351|5|Briefly described|Plate 4 (in pocket)|Late Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province: Gascoyne Platform/Sub-basin.||||||13-DEC-07
271|Alinga Formation|24410|5|Briefly described|p132|Cretaceous|Cretaceous|of the Winning Group. Glauconite-rich clayey siltstone to greensand, rarely exposed. Overlies the Windalia Radiolarite. Geological Province: Carnarvon Basin.||||||24-NOV-09
271|Alinga Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
271|Alinga Formation|35057|5|Briefly described|p301|||||||||
271|Alinga Formation|36257|6|Mentioned|Table 2.1|||||||||
271|Alinga Formation|36890|3|Fully described|p297|||Formerly Alinga Beds and Alinga Greensand.||||||31-MAY-06
271|Alinga Formation|38485|4|Described|p16|||||||||
271|Alinga Formation|38998|4|Described|p18|||||||||
271|Alinga Formation|39158|6|Mentioned|p37|||||||||
271|Alinga Formation|39211|6|Mentioned|p58|||||||||
271|Alinga Formation|40340|5|Briefly described|p14|||||||||
271|Alinga Formation|40341|6|Mentioned|Map legend|Turonian|Cenomanian|Turonian - Cenomanian||||||
271|Alinga Formation|40342|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
271|Alinga Formation|40343|5|Briefly described|p12|||||||||
271|Alinga Formation|40617|6|Mentioned|p18|||||||||
271|Alinga Formation|41271|3|Fully described|p156|||||||||
271|Alinga Formation|41438|6|Mentioned|p109|||||||||
271|Alinga Formation|41639|6|Mentioned|p14|||||||||
271|Alinga Formation|42116|5|Briefly described|p18|||See also Fig.1||||||
271|Alinga Formation|42123|4|Described|p15|||||||||
271|Alinga Formation|42393|5|Briefly described|p103|||||||||
271|Alinga Formation|42598|5|Briefly described|P 95|||||||||
271|Alinga Formation|42995|4|Described|p15|||see also Table 1.||||||
271|Alinga Formation|43598|5|Briefly described|p813|||||||||
271|Alinga Formation|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
271|Alinga Formation|49942|5|Briefly described|p11|Late Cretaceous|Late Cretaceous|Coeval with Gearle Siltstone. Overlies Windalia Radiolarite. Of the Winning Group. Geological Province: Gascoyne Platform.||||||22-FEB-05
271|Alinga Formation|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|||||||
271|Alinga Formation|61811|4|Described|p3 Fig.2, p9 Table 3, p11, pp13-15, p62.|Albian|Albian|Northern Perth Basin. Planolites, Chondrites and Zoophycus are the dominant ichnofacies. Upper part of this unit is equivalent to upper Gearle Siltstone. Type section details in Appendix 1.||Unit in Winning Group.||Overlies Windalia Radiolarite. Is overlain disconformably by Toolonga Calcilutite.|Friable muddy glauconitic siltstone and fine- to medium-grained greensand; belemnite guards locally abundant.|
271|Alinga Formation|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||
271|Alinga Formation|63068|5|Briefly described|p46|||Coeval with Gearle Siltstone. Geological Province: southern Carnarvon Basin.||||||07-FEB-08
271|Alinga Formation|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
271|Alinga Formation|64635|5|Briefly described|p4 Fig.3, p7 |Albian|Albian|||Unit in Winning Group.||||
271|Alinga Formation|67200|5|Briefly described|p8 fig 6, p17 table 1, p50, p53|Cretaceous|Cretaceous|Thermal conductivity of 1.00 W/mK||Winning Group||Overlies Windalia Radiolarite, unconformably overlain by Toolonga Calcilutite|Crudely bedded siltstone.|
271|Alinga Formation|67340|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|Northern Perth Basin.||Winning Group.||||
271|Alinga Formation|68206|6|Mentioned|p32|Albian|Albian|Carnarvon Basin.||||||
271|Alinga Formation|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
271|Alinga Formation|69182|6|Mentioned|Ch3 p12|||Carnarvon Basin.||||Overlies the Windalia Radiolarite.||
271|Alinga Formation|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.||||
437|Angalarri Siltstone|14019|4|Described|p16|Neoproterozoic|Neoproterozoic|Of the Auvergne Group. Predominantly siltstone and shale. Overlies the Jasper Gorge Sandstone; unconformably overlain by the Fargoo Tillite. Age: 838 +/-80Ma (Rb-Sr, Webb and Page 1977). Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|22547|5|Briefly described|Fig4,p25|||Of the Auvergne Group. Geological province: Victoria River Basin. Overlies Jasper Gorge Sandstone, overlain by Upper Auvergne Group.||||||14-NOV-06
437|Angalarri Siltstone|23937|6|Mentioned|p84 App.1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|24122|3|Fully described|p10, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlies Jasper Gorge Sandstone, conformably overlain by Saddle Creek Formation.  Maximum thickness 753m (on AUVERGNE).  Geological Province: Victoria Basin.||||||25-JAN-10
437|Angalarri Siltstone|24297|5|Briefly described|p4|Proterozoic|Proterozoic|Of Auvergne Group. Overlain by Saddle Creek Formation, overlies Jasper Creek Formation.  Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Parent: Auvergne Group.   Geological Province: Victoria Basin||||||
437|Angalarri Siltstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Overlies Jasper Gorge Sandstone; overlain by Saddle Creek Formation. Geological Province: Victoria Basin||||||25-JAN-06
437|Angalarri Siltstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.  Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|28255|3|Fully described|p66, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Of the Auvergne Group.  Deep water sediments - of siltstone, sandstone, minor shale and limestone. Conformably overlies Jasper Gorge Sandstone; conformably underlies Saddle Creek Formation. max. thickness: >230m.  See also p68 Tb.6 and p139 Appendix.||||||07-JUN-05
437|Angalarri Siltstone|32170|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
437|Angalarri Siltstone|32172|4|Described|Table 1|||Adelaidean||||||
437|Angalarri Siltstone|32173|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Khaki and green siltstone with sandstone interbeds.||||||16-NOV-04
437|Angalarri Siltstone|32307|4|Described|Table 2|||Proterozoic||||||
437|Angalarri Siltstone|32309|6|Mentioned|Map legend|Carpentarian|Carpentarian|Adelaidean/Carpentarian||||||
437|Angalarri Siltstone|32310|6|Mentioned|Map legend|Adelaidean|Adelaidean|Adelaidean/Carpentarian.||||||
437|Angalarri Siltstone|32660|5|Briefly described|Table 6|||||||||
437|Angalarri Siltstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.||||||02-DEC-04
437|Angalarri Siltstone|32700|4|Described|p14|||See also Table 1||||||
437|Angalarri Siltstone|32701|4|Described|Table 1|||Adelaidean. See also p9||||||17-JUL-06
437|Angalarri Siltstone|32728|6|Mentioned|Fig.14|||||||||
437|Angalarri Siltstone|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||02-DEC-04
437|Angalarri Siltstone|33373|4|Described|p10|||Table 2.||||||
437|Angalarri Siltstone|33375|6|Mentioned|p6|||||||||26-APR-05
437|Angalarri Siltstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
437|Angalarri Siltstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Khaki and green siltstone, interbeds of fine sandstone and shale; minor limestone.||||||27-APR-05
437|Angalarri Siltstone|38157|6|Mentioned|p284|||||||||
437|Angalarri Siltstone|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
437|Angalarri Siltstone|40105|6|Mentioned|p313|||||||||
437|Angalarri Siltstone|40494|6|Mentioned|p10|||||||||
437|Angalarri Siltstone|40765|6|Mentioned|p11|||||||||
437|Angalarri Siltstone|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Siltstone, fissile, reddish-brown to light-green; some dolomitic siltstone layers (160m proved in drillhole NTGS 83/1).||||||07-OCT-05
437|Angalarri Siltstone|41661|3|Fully described|p19|||||||||
437|Angalarri Siltstone|45022|14|Not recorded|p87,88 tb11,12||Adelaidean|Unit of Victoria River Group pl3,28||||||
437|Angalarri Siltstone|45112|5|Briefly described|Table 15|||||||||
437|Angalarri Siltstone|48938|2|Defined|p36|Adelaidean|Adelaidean|Measured section pp93||||||17-JUL-06
437|Angalarri Siltstone|48942|3|Fully described|p66|||Strat. section pp115 & 116||||||17-JUL-06
437|Angalarri Siltstone|48943|3|Fully described|p75|||Strat. section p138.||||||17-JUL-06
437|Angalarri Siltstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlies Jasper Gorge Sandstone. Overlain by Saddle Creek Formation. Siltstone, shale, minor dolostone and sandstone||||||
437|Angalarri Siltstone|60682|4|Described|piii, 8|Cryogenian|Cryogenian|Correlated with Helicopter Siltstone. Thickness: 753m. Conformably overlies Jasper Gorge Sandstone. Conformably overlain by Saddle Creek Formation. Age: 838 +/- 80Ma. Siltstone, shale and sandstone. Of Auvergne Group. Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|60685|5|Briefly described|p4 Figure 3|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Jasper Gorge Sandstone. Age: 838 +/- 80Ma (controversial?). Geological Province: Victoria Basin.||||||
437|Angalarri Siltstone|61573|5|Briefly described|p676, p678 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of Auvergne Group. Siltstone, shale, minor sandstone and dolostone. Conformably overlies Jasper Gorge Sandstone. Age: 821+/-80Ma. Thickness in Bullo River 1 drillhole: 753m. Geol. Prov: Victoria Basin. ||||||
437|Angalarri Siltstone|65331|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Auvergne Group, Victoria Basin. Siltstone, shale, minor dolostone and sandstone||||||02-FEB-10
437|Angalarri Siltstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Overlies Jasper Gorge Sandstone. Is overlain by Saddle Creek Formation.||
437|Angalarri Siltstone|65417|5|Briefly described|p159.|||Victoria River Basin. Age from Webb and Page (1977).|838 +/- 142 Ma (Rb-Sr whole rock).|Unit in Auvergne Group.||||
437|Angalarri Siltstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Overlies Jasper Gorge Sandstone. Is overlain by Saddle Creek Formation.|Siltstone, interbeds of fine sandstone and shale; minor limestone, dolostone.|
437|Angalarri Siltstone|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Auvergne Group.|||Siltstone, shale, minor dolostone and sandstone.|
437|Angalarri Siltstone|68733|5|Briefly described|p179 Tb.1, p183, p185-186, p189, p1921|Cryogenian|Cryogenian|Victoria Basin. See also Angalarri Sandstone. Sm-Nd isotope data tabulated.||Auvergne Group.||Conformably overlies the Jasper Gorge Sandstone. Correlated with Bitter Springs Formation and Eliot Range Dolomite.||04-DEC-17
437|Angalarri Siltstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Overlies Jasper Gorge Sandstone. Is overlain by Saddle Creek Formation.||12-JUL-16
437|Angalarri Siltstone|69441|5|Briefly described|p26:1-4, 6|Neoproterozoic|Neoproterozoic|Underlies the Whirlwind Plain. Over 300m thick in outcrop; 753m in Bullo River 1. Relatively deep-water deposits, hummocky cross-stratification below storm wave base. Rb-Sr whole rock age. Contains pyritic shale units; may be prospective for stratiform sediment-hosted base metal mineralisation. Pods and veins of barite occur, but no commercial exploitation has been reported.|838 +/- 80 Ma (Webb and Page, 1977).|Auvergne Group.||Conformably overlies Jasper Gorge Sandstone. Is overlain conformably (locally unconformably) by Saddle Creek Formation.|Siltstone and shale, minor dolostone and sandstone, more arenaceous in SW. Local lateral and vertical variations include dolomitic, glauconitic, pyritic and carbonaceous facies.|12-JUL-16
437|Angalarri Siltstone|69442|6|Mentioned|p27:2; 3 Tb.27.1; 5|||||Auvergne Group.||Is overlain unconformably by Uniya Formation and Skinner Sandstone.||12-JUL-16
437|Angalarri Siltstone|69445|6|Mentioned|p30:10|||Is displaced c.100m by the West Baines Fault.||||||12-JUL-16
437|Angalarri Siltstone|69673|5|Briefly described|p188|||753m thick. ||Auvergne Group|||Micaceous fissile siltstone/mudstone and lesser sandstone.|
437|Angalarri Siltstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Siltstone, shale, minor dolostone and sandstone.|
437|Angalarri Siltstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group||Overlies Jasper Gorge Sandstone. Is overlain by Saddle Creek Formation, Moonlight Valley Tillite, Kinevans Sandstone.|Siltstone, interbeds of fine sandstone and shale; minor limestone, dolostone.|
437|Angalarri Siltstone|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Conformably overlies Jasper Gorge Sandstone. Is overlain conformably by Saddle Creek Formation.|Siltstone, shale, minor dolostone and sandstone.|
437|Angalarri Siltstone|70968|5|Briefly described|p124|Neoproterozoic|Neoproterozoic|Victoria Basin. Rb-Sr wholerock age.|838 +/- 80 Ma (Webb and Page, 1977).|Auvergne Group.||||
437|Angalarri Siltstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone|
437|Angalarri Siltstone|71302|4|Described|p1,6-7,43-50,72,74|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Maximum thickness of 753m on AUVERGNE 1:250 000 map sheet. Interpreted as a moderately deep water, sub-wavebase shelf deposit on the basis of micro-hummocky cross stratification, common flute casts, well defined lamination and ripple morphologies. (Dunster et al., 2000). Webb and Page (1977) provided Rb-Sr whole rock isochron age of 838+\-80 Ma, and the only existing estimate of age of Auvergne Group. Sample GA 1957132 (quartz sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1147+\-26 Ma. Dominated by detritus in the range 1550-1650 Ma, and have very little pre-1800 Ma zircon. Sample location, description, zircon description and SHRIMP analyses are provided.||Unit of Auvergne Group.||Overlain conformably by Saddle Creek Formation. Underlain by Jasper Gorge Sandstone.|Micaceous siltstone/mudstone and lesser sandstone.|09-DEC-19
437|Angalarri Siltstone|71893|5|Briefly described|p69|||Rb-Sr whole rock age is derived from Webb and Page, 1977.|838 +/- 80 Ma (Rb-Sr whole rock)|Auvergne Group||||
437|Angalarri Siltstone|73083|6|Mentioned|p7, p48||||||||Siltstone, shale, minor dolostone, sandstone, and dolarenite.|
464|Anketell Formation|7433|6|Mentioned|p42 Fig.30. |Cretaceous|Cretaceous|Marine clastics. Mis-named for Anketell Sandstone.||||||
464|Anketell Formation|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
464|Anketell Formation|32979|6|Mentioned|p38|||Correlation with basins in India||||||
464|Anketell Formation|33165|6|Mentioned|p57|||Refers Veevers & Wells (1961)||||||
464|Anketell Formation|34363|6|Mentioned|p56|||See Fig.7. Tithonian.||||||
464|Anketell Formation|35202|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
464|Anketell Formation|35969|6|Mentioned|Table 7|||||||||
464|Anketell Formation|43563|6|Mentioned|Fig2, p5|Albian|Aptian|||||||07-OCT-20
464|Anketell Formation|43656|6|Mentioned|Fig.2,p8|Albian|Aptian|||||||
464|Anketell Formation|43746|6|Mentioned|Fig.2,p11|Albian|Aptian|||||||
464|Anketell Formation|44998|2|Defined|p.154-7|||Replaces "Anketell Sandstone". Overlies Callawa Formation. Overlain by Frezier Sandstone. p.119,123-7,133,158-164,168,map. See also App.2 p271.||||||
464|Anketell Formation|45149|6|Mentioned|Table 1|||Page 15.||||||
464|Anketell Formation|45153|2|Defined|App.8-137|Aptian|Aptian|Formerly Anketell Sandstone. See also App.6-95. Type Section: Hill T7, at 22degrees08'S, 124degrees20'E (Traves & others, 1956, p. 28). Veevers & Wells ( 1961, p. 157) ?redefined the unit and selected A11 (221. in. Table 6) as the new type section (20degrees26'30"S, 122degrees32'30"E) of the Anketell Formation. Veevers & Wells (1961) considered that the T7 exposure is part of the Kidson beds.Lithology: claystone, shale, and siltstone with thin lenses of conglomerate.||||||13-DEC-22
464|Anketell Formation|46319|6|Mentioned|p18|||Now known as Parda Formation.  Geological Province: Canning Basin.||||||
464|Anketell Formation|64580|4|Described|map legend|Early Cretaceous|Early Cretaceous|Fine-grained sandstone and siltstone; lesser coarse -grained sandstone and conglomerate.||||||09-DEC-08
464|Anketell Formation|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
464|Anketell Formation|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||23-FEB-10
464|Anketell Formation|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Parda Formation.||
464|Anketell Formation|67202|6|Mentioned|p126, p135|||See also Anketell Sandstone.||||||
464|Anketell Formation|68007|6|Mentioned|p4, Plate 1|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies Callawa Formation.||25-FEB-20
464|Anketell Formation|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Parda Formation, Melligo Sandstone.||
464|Anketell Formation|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p45|||Canning Basin. ||||Overlies the Frezier and Melligo Sandstones and the Parda Formation.||
464|Anketell Formation|69590|4|Described|500k_geologyp08_lut.csv|Early Cretaceous|Early Cretaceous||||||fine-grained sandstone and siltstone; lesser coarse -grained sandstone and conglomerate|
464|Anketell Formation|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Parda Formation and the Melligo Sandstone.||10-FEB-20
464|Anketell Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sandstone|
464|Anketell Formation|71894|5|Briefly described|p3-p4|Cretaceous|Jurassic|Canning Basin. Relatively uniform in thickness from north to south but thins from the west to the east.||||Overlies the Frezier Sandstone, Melligo Sandstone and the Parda Formation.|Sandstone and shale.|
464|Anketell Formation|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Canning Basin.|||||Fine-grained sandstone and siltstone; lesser coarse-grained sandstone and conglomerate.|
464|Anketell Formation|72497|5|Briefly described|p3 Fig.2.|Albian|Aptian|Shown, along with Bejah claystone, as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform.||||Laterally equivalent to Bejah Claystone. Conformably overlies Samuel Formation and Melligro-Para-Frozier Sandstone.||
464|Anketell Formation|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Broome Platform.||||Overlies Frezier and Melligo Sandstones, Parda Formation. Laterally equivalent to Bejah Claystone.|Includes sandstone and some shale.|
464|Anketell Formation|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Frezier Sandstone, Parda Formation and Melligo Sandstone. Equivalent to Bejah Claystone.|Dominantly sandstone with lesser shale.|
488|Antrim Plateau Volcanics|9324|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group. Basalt and porphyritic basalt with some interlayered subarkose.||||||
488|Antrim Plateau Volcanics|9538|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Purple to black, commonly weathered. fine to medium-grained basalt, vesicular in places: minor red ferruginous medium to coarse sandstone interbeds near base in places; rare jasper.||||||28-OCT-04
488|Antrim Plateau Volcanics|9579|5|Briefly described|Map Sheet|Ordovician|Cambrian|||||||
488|Antrim Plateau Volcanics|12891|5|Briefly described|p731, p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: Wiso Basin.||||||07-FEB-11
488|Antrim Plateau Volcanics|13194|4|Described|p382, p395, p399.|Early Cambrian|Early Cambrian|See Table 4-16 and Figures 4-59 and 4-63. 0-155m thick subaerial volcanic flows, eolian clastics. Type Section: Sprink Creek area (Ord Basin).||||Overlain by Carlton Group.|Eolian sandstone overlain by 2 to 4 tholeiitic basalt flows.|
488|Antrim Plateau Volcanics|13234|6|Mentioned|p248, p252 Fig.4|||Erupted during rifting at start of Petrel Sub-basin.||||||
488|Antrim Plateau Volcanics|14019|3|Fully described|p19-20|Early Cambrian|Early Cambrian|Contains the Mount Close Chert Member. Consists of 20-60m thick lava flows, mostly fine basalt with conspicuous vesicular flow tops, and less commonly plagioclase-phyric basalt. Max. thickness: 1000m. Geological Province: Ord Basin.||||||17-MAY-06
488|Antrim Plateau Volcanics|14228|6|Mentioned|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|22440|5|Briefly described|p5||Early Cambrian|||||||
488|Antrim Plateau Volcanics|22446|6|Mentioned|p20|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|22496|6|Mentioned|p10||Early Cambrian|||||||16-AUG-04
488|Antrim Plateau Volcanics|22537|6|Mentioned|34|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|22547|4|Described|p29||Early Cambrian|Geol.Prov: Goose Hole Group, Ord and Bonaparte Basins. Age: c. 540 Ma. 1000 m thick. Overlain by Headleys Limestone||||||18-JUL-06
488|Antrim Plateau Volcanics|22650|6|Mentioned|p 159|Early Cambrian|Early Cambrian|Province - Wilso Basin.||||||
488|Antrim Plateau Volcanics|22716|5|Briefly described|table4, p239|Early Cambrian|Neoproterozoic III|||||||
488|Antrim Plateau Volcanics|22754|5|Briefly described|p10|Paleozoic|Neoproterozoic|Geological Province: Ord Basin.||||||07-NOV-08
488|Antrim Plateau Volcanics|22809|5|Briefly described|1|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|22813|5|Briefly described|Map|Ordovician|Cambrian|Basalt.||||||19-OCT-05
488|Antrim Plateau Volcanics|22814|5|Briefly described|p245, fig2|Cambrian|Neoproterozoic|In Ord basin and Southern Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|23125|5|Briefly described|Table.1||Cambrian|Age: Lower Cambrian.||||||
488|Antrim Plateau Volcanics|23216|4|Described|p3,Table1p7, p33, p35-7||Early Cambrian|Present name: Traves (1955); Former name: Antrim Plateau Basalts by David (1932).||||||19-JAN-06
488|Antrim Plateau Volcanics|23314|5|Briefly described|329|Early Cambrian|Neoproterozoic|||||||
488|Antrim Plateau Volcanics|23328|4|Described|1029-1038|Early Cambrian|Early Cambrian|Age: 545-509Ma[?].  K-Ar age ranges given as 402-515Ma.||||||07-SEP-09
488|Antrim Plateau Volcanics|23374|6|Mentioned|p23|||||||||
488|Antrim Plateau Volcanics|23377|6|Mentioned|p212 Fig.5||Early Cambrian|of Vulcan Sub-basin.||||||
488|Antrim Plateau Volcanics|23383|5|Briefly described|p22, p13||Cambrian|Massive, vesicular and amygdaloidal basalt, with occasional sandstone interbeds.  Conformably overlie the Lally Conglomerate. Max. thickness: 1500m.  Geological Province: Ord Basin.   See also p5 Tb. 1, p6 Fig. 3.||||||25-JAN-05
488|Antrim Plateau Volcanics|23516|6|Mentioned|p598|||||||||
488|Antrim Plateau Volcanics|23599|4|Described|p19|Cambrian|Cambrian|Age: c.540 Ma. Underlying unit Lally Conglomerate. Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|23601|5|Briefly described|Map legend|Cambrian|Cambrian|Dark grey, vesicular and amygdaloidal basalt; generally weakly weathered.||||||25-JAN-05
488|Antrim Plateau Volcanics|23621|4|Described|p35|Cambrian|Cambrian|See also page 9 table 1. Overlying unit Windoo Sandstone. Underlying unit Albert Edward Group. Geological Province: Ord Basin. Max. thickness: 500 m.||||||
488|Antrim Plateau Volcanics|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Ord Basin||||||
488|Antrim Plateau Volcanics|23714|5|Briefly described|p36|Cambrian|Cambrian|See also page 7 Table 1. Max. thickness: 45 m.||||||
488|Antrim Plateau Volcanics|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
488|Antrim Plateau Volcanics|23770|5|Briefly described|p2 Fig. 1|Early Cambrian|Early Cambrian|Massive and amygdaloidal tholeiitic basalt.  Geological Province: Daly River Basin.||||||16-JUL-13
488|Antrim Plateau Volcanics|23806|5|Briefly described|p1122|Cambrian|Proterozoic|Underlain by Louisa Downs Group.||||||
488|Antrim Plateau Volcanics|23820|5|Briefly described|p202|Early Cambrian|Early Cambrian|Geological Province: Bonaparte Gulf Basin.||||||
488|Antrim Plateau Volcanics|23821|4|Described|p244|Early Cambrian|Late Adelaidean|Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|23858|5|Briefly described|p919|||Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|23914|5|Briefly described|p158 Fig. 12|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|23937|4|Described|p53, p26 Fig. 12|Early Cambrian|Early Cambrian|Succession of mainly basaltic and minor sedimentary rocks.  Outcrop extensively in KATHERINE.  Geological Province: Daly Basin.||||||
488|Antrim Plateau Volcanics|24047|6|Mentioned|p62|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|24066|5|Briefly described|p237|Early Cambrian|Early Cambrian|Geological Province: Wiso Basin.||||||
488|Antrim Plateau Volcanics|24111|5|Briefly described|p217|Early Cambrian|Early Cambrian|Age: c.513+/-12Ma (Hanley and Wingate, 2000).||||||
488|Antrim Plateau Volcanics|24122|3|Fully described|p12|Cambrian|Cambrian|Sandstone, siltstone, dolostone, conglomerate, dolarenite.  Overlies Tijunna and Auvegne Groups. Geological Province: Wiso Basin.||||||25-JAN-10
488|Antrim Plateau Volcanics|24173|5|Briefly described|p24|Cambrian|Cambrian|Unconformably overlies Albert Edward Group. Geological Province: Ord Basin||||||06-APR-05
488|Antrim Plateau Volcanics|24297|4|Described|p17|Early Cambrian|Early Cambrian|Age: 545-509Ma. Geological Province: Wiso Basin.||||||
488|Antrim Plateau Volcanics|24298|5|Briefly described|Map Legend|Cambrian|Cambrian|Porphyritic tholeiitic basalt, agglomerate, quartz sandstone, chert, limestone.||||||19-OCT-05
488|Antrim Plateau Volcanics|24300|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|24303|6|Mentioned|p62 Appendix|||Of the Ord, Daly and western Wiso Basins. Formerly Antrim Plateau Basalts of David (1932). Correlates with the Helen Springs and Milliwindi Dolerite.||||||
488|Antrim Plateau Volcanics|24390|5|Briefly described|p2 Fig. 2|Cambrian||Geological Province: Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|24441|6|Mentioned|p1|Cambrian|Cambrian|Victoria Basin is blanketed by these rocks.||||||
488|Antrim Plateau Volcanics|24503|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Ord and Bonaparte Basins.||||||
488|Antrim Plateau Volcanics|24569|5|Briefly described|p248 Fig. 3|Middle Cambrian|Early Cambrian|Geological Province: Petrel Sub-basin.||||||
488|Antrim Plateau Volcanics|24578|6|Mentioned|p792|Cambrian|Cambrian|Age: ~510 Ma||||||
488|Antrim Plateau Volcanics|28255|3|Fully described|p81|Cambrian|Cambrian|Supersedes A.P.Basalts. Sequence of basalt flows with thin interbeds of sst, chert, lst, and sltst; massive, porphyritic and vesicular tholeiitic basalt. Unconformable below Montejinni Lst.,Negro Gp. and Mullaman Beds; overlies Killaloc Fm.||||||16-JUL-13
488|Antrim Plateau Volcanics|29474|6|Mentioned|p7|||||||||
488|Antrim Plateau Volcanics|29591|5|Briefly described|p122|||||||||
488|Antrim Plateau Volcanics|29804|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|29805|4|Described|Table 1|||||||||
488|Antrim Plateau Volcanics|29807|6|Mentioned|p13|||||||||
488|Antrim Plateau Volcanics|29809|6|Mentioned|Table 1|||||||||
488|Antrim Plateau Volcanics|29811|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|29812|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|29817|6|Mentioned|p13|||||||||
488|Antrim Plateau Volcanics|30003|4|Described|p11, p13|Early Cambrian|Early Cambrian|Consist of a series of basalt lava flows with thin interbeds of sandstone, chert, silicified carbonate rocks, limestone, and pyroclastic rocks. Overlain by Montejinni Limestone.||||||19-APR-05
488|Antrim Plateau Volcanics|30004|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|30660|6|Mentioned|Table 1|||Cambrian age||||||
488|Antrim Plateau Volcanics|30661|6|Mentioned|Table 1|||||||||
488|Antrim Plateau Volcanics|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
488|Antrim Plateau Volcanics|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
488|Antrim Plateau Volcanics|30895|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|31361|4|Described|Table 1|||||||||
488|Antrim Plateau Volcanics|31362|6|Mentioned|Table 1|||||||||
488|Antrim Plateau Volcanics|31412|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|31577|6|Mentioned|p76|||Stratigraphy||||||
488|Antrim Plateau Volcanics|31917|6|Mentioned|p32|||L.Cambrian. See Table 1||||||
488|Antrim Plateau Volcanics|32106|6|Mentioned|p305|||Palaeomagnetic data||||||
488|Antrim Plateau Volcanics|32107|6|Mentioned|p409|||Palaeomagnetic results||||||
488|Antrim Plateau Volcanics|32109|3|Fully described|p192|||L.Cambrian. See also p93-196||||||18-JUL-06
488|Antrim Plateau Volcanics|32170|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|32172|4|Described|Table 2|||See also p10. Lower Cambrian||||||18-JUL-06
488|Antrim Plateau Volcanics|32173|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Massive porphyritic and tholeiitic basalt.  Overlain by Negri Group rocks.||||||17-NOV-04
488|Antrim Plateau Volcanics|32175|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||||02-DEC-04
488|Antrim Plateau Volcanics|32469|6|Mentioned|p533|||||||||
488|Antrim Plateau Volcanics|32648|6|Mentioned|p32|||Lower Cambrian.||||||
488|Antrim Plateau Volcanics|32659|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|32660|6|Mentioned|p244|||Fig.6||||||
488|Antrim Plateau Volcanics|32664|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Briefly described in notesProb.Lower Cambrian||||||
488|Antrim Plateau Volcanics|32699|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||||02-DEC-04
488|Antrim Plateau Volcanics|32700|4|Described|Table 2|||See also p15. Refers Traves (1955)||||||18-JUL-06
488|Antrim Plateau Volcanics|32701|4|Described|Table 2|||See also p15. Lower Cambrian||||||18-JUL-06
488|Antrim Plateau Volcanics|32728|6|Mentioned|Fig.3|||||||||
488|Antrim Plateau Volcanics|32775|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|||||||02-DEC-04
488|Antrim Plateau Volcanics|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969)||||||
488|Antrim Plateau Volcanics|33004|6|Mentioned|p89|||||||||
488|Antrim Plateau Volcanics|33373|3|Fully described|p10|||Table 3.||||||
488|Antrim Plateau Volcanics|33374|4|Described|p13|||Strat. table p1.||||||18-JUL-06
488|Antrim Plateau Volcanics|33375|6|Mentioned|p13, p11 Tb. 1|||Consist of numerous basalt flows averaging about 30m in thickness, with thin interbeds of chert and sandstone. Includes the Blackfella Rockhole Member. Lower Cambrian or Upper Adelaidean.||||||27-APR-05
488|Antrim Plateau Volcanics|33376|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|33377|5|Briefly described|Table 2|||Re stratigraphy||||||
488|Antrim Plateau Volcanics|33378|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Massive and porphyritic basalt, vesicular and amygdaloidal in places.||||||27-APR-05
488|Antrim Plateau Volcanics|33443|6|Mentioned|p260|||||||||
488|Antrim Plateau Volcanics|33622|6|Mentioned|p88|||Early Camb.||||||
488|Antrim Plateau Volcanics|33625|6|Mentioned|p187|||||||||
488|Antrim Plateau Volcanics|33738|6|Mentioned|p42|||||||||
488|Antrim Plateau Volcanics|34051|4|Described|Table 1|||Lower Cambrian.||||||18-JUL-06
488|Antrim Plateau Volcanics|34052|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|34053|6|Mentioned|p8|||L.Cambrian||||||
488|Antrim Plateau Volcanics|34162|3|Fully described|p119|||Early Cambrian||||||
488|Antrim Plateau Volcanics|34230|6|Mentioned|Plate 8|Cambrian|Cambrian|Basalt and agglomerate, red-brown sandstone and chert.||||||28-OCT-04
488|Antrim Plateau Volcanics|34438|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|34439|4|Described|Table 1|||Lower Cambrian. See also pp6,8,11,14||||||18-JUL-06
488|Antrim Plateau Volcanics|34440|4|Described|Table 1|||Lower Cambrian. See also pp6,9||||||18-JUL-06
488|Antrim Plateau Volcanics|34441|6|Mentioned|p11|||See also P12. L.Camb. (666+-56my)||||||
488|Antrim Plateau Volcanics|34737|6|Mentioned|p355|||||||||
488|Antrim Plateau Volcanics|34810|5|Briefly described|p5|||||||||
488|Antrim Plateau Volcanics|34834|6|Mentioned|p226|||||||||
488|Antrim Plateau Volcanics|34945|6|Mentioned|p356|||||||||
488|Antrim Plateau Volcanics|34983|6|Mentioned|p32|||||||||
488|Antrim Plateau Volcanics|35054|6|Mentioned|p249|||||||||
488|Antrim Plateau Volcanics|35055|6|Mentioned|p222|||||||||
488|Antrim Plateau Volcanics|35088|6|Mentioned|Fig.8|||||||||
488|Antrim Plateau Volcanics|35229|6|Mentioned|p6|||||||||
488|Antrim Plateau Volcanics|35231|4|Described|Table.1|||||||||
488|Antrim Plateau Volcanics|36014|6|Mentioned|p151|||||||||
488|Antrim Plateau Volcanics|36257|6|Mentioned|Table 2.1|||||||||
488|Antrim Plateau Volcanics|36335|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|36532|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|36551|6|Mentioned|Table 16|||See also P22.||||||
488|Antrim Plateau Volcanics|36890|3|Fully described|p395|||||||||
488|Antrim Plateau Volcanics|36892|5|Briefly described|p451|||||||||
488|Antrim Plateau Volcanics|36898|6|Mentioned|p183|||||||||
488|Antrim Plateau Volcanics|36904|6|Mentioned|p6|||||||||
488|Antrim Plateau Volcanics|37577|6|Mentioned|p70|||||||||
488|Antrim Plateau Volcanics|37818|6|Mentioned|Table 2|||||||||
488|Antrim Plateau Volcanics|38157|6|Mentioned|Table X|||||||||
488|Antrim Plateau Volcanics|38988|6|Mentioned|Fig.4|||||||||
488|Antrim Plateau Volcanics|39210|3|Fully described|p46|||See also p85||||||18-JUL-06
488|Antrim Plateau Volcanics|39523|6|Mentioned|p95|||||||||
488|Antrim Plateau Volcanics|39679|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
488|Antrim Plateau Volcanics|39827|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Prob.Early Cambrian||||||
488|Antrim Plateau Volcanics|40494|4|Described|p13|||||||||
488|Antrim Plateau Volcanics|40792|6|Mentioned|p174|||||||||
488|Antrim Plateau Volcanics|40957|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|40993|6|Mentioned|p4|||||||||
488|Antrim Plateau Volcanics|41158|6|Mentioned|p21|||||||||
488|Antrim Plateau Volcanics|41268|6|Mentioned|p297|||||||||
488|Antrim Plateau Volcanics|41294|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|41295|4|Described|p19|||||||||
488|Antrim Plateau Volcanics|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
488|Antrim Plateau Volcanics|41453|6|Mentioned|p245|||||||||
488|Antrim Plateau Volcanics|41459|6|Mentioned|Fig.2|||||||||
488|Antrim Plateau Volcanics|41557|6|Mentioned|p589|||||||||
488|Antrim Plateau Volcanics|41586|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
488|Antrim Plateau Volcanics|41598|6|Mentioned|p413|||||||||
488|Antrim Plateau Volcanics|41645|6|Mentioned|Fig.4|||||||||
488|Antrim Plateau Volcanics|41646|6|Mentioned|Map legend|Cambrian|Ordovician|Basalt, sandstone.||||||14-OCT-05
488|Antrim Plateau Volcanics|41660|5|Briefly described|Map legend|Ordovician|Cambrian|Basalt, massive and vesicular; interlayered micaceous siltstone or mudstone; laterised carbonate rocks(? limestone); lenticular interlayered and cross cutting 'dykes' of sometimes flaggy feldspathic quartz arenite. Max thickness: 80m.||||||07-OCT-05
488|Antrim Plateau Volcanics|41661|4|Described|p23|||||||||
488|Antrim Plateau Volcanics|41663|6|Mentioned|p44|||||||||
488|Antrim Plateau Volcanics|41690|5|Briefly described|p3|||||||||
488|Antrim Plateau Volcanics|41731|6|Mentioned|Fig.2|||||||||
488|Antrim Plateau Volcanics|41840|2|Defined|p38|Early Cambrian||||||||
488|Antrim Plateau Volcanics|41864|3|Fully described|p9|Early Cambrian||Formerly Antrim Plateau Basalts. Age inferred.||||||
488|Antrim Plateau Volcanics|41865|6|Mentioned|Map Legend|Early Cambrian||||||||
488|Antrim Plateau Volcanics|41866|5|Briefly described|Map legend|Early Cambrian||||||||
488|Antrim Plateau Volcanics|41883|6|Mentioned|p65|||||||||
488|Antrim Plateau Volcanics|42012|6|Mentioned|p29|||||||||
488|Antrim Plateau Volcanics|42014|5|Briefly described|Map legend|Cambrian|Ordovician|||||||
488|Antrim Plateau Volcanics|42056|4|Described|p93|||||||||
488|Antrim Plateau Volcanics|42059|6|Mentioned|Fig.2 P131|||||||||
488|Antrim Plateau Volcanics|42070|6|Mentioned|Fig.8 P11|||||||||
488|Antrim Plateau Volcanics|42175|5|Briefly described|Fig.2 P200|||||||||
488|Antrim Plateau Volcanics|42191|5|Briefly described|Fig.7 P140|||||||||
488|Antrim Plateau Volcanics|42442|6|Mentioned|p31|||||||||
488|Antrim Plateau Volcanics|42504|6|Mentioned|p84|||||||||
488|Antrim Plateau Volcanics|42639|6|Mentioned|p46|||||||||
488|Antrim Plateau Volcanics|42768|6|Mentioned|Fig.6|||||||||
488|Antrim Plateau Volcanics|42771|5|Briefly described|p15, Fig.16|||||||||
488|Antrim Plateau Volcanics|42778|5|Briefly described|p14|||||||||
488|Antrim Plateau Volcanics|43010|6|Mentioned|p140|||of "Mid Proterozoic" age.||||||
488|Antrim Plateau Volcanics|43011|6|Mentioned|Table 2,p12|||||||||
488|Antrim Plateau Volcanics|43140|4|Described|p4|Ordovician|Cambrian|||||||
488|Antrim Plateau Volcanics|43149|5|Briefly described|Map Legend||Cambrian|||||||
488|Antrim Plateau Volcanics|43187|5|Briefly described|p2|||||||||
488|Antrim Plateau Volcanics|43236|6|Mentioned|p13,Fig.12.||Cambrian|||||||
488|Antrim Plateau Volcanics|43281|6|Mentioned|Map legend||Cambrian|||||||
488|Antrim Plateau Volcanics|43299|5|Briefly described|Map Legend||Cambrian|of Negri Subgroup.||||||
488|Antrim Plateau Volcanics|43301|5|Briefly described|Map Legend||Cambrian|of Mahoney Group.||||||
488|Antrim Plateau Volcanics|43302|5|Briefly described|Map Legend||Cambrian|||||||
488|Antrim Plateau Volcanics|43442|6|Mentioned|p21-23,25||Cambrian|||||||
488|Antrim Plateau Volcanics|43560|6|Mentioned|fig.1,p227|||||||||
488|Antrim Plateau Volcanics|43561|6|Mentioned|p1443|||||||||
488|Antrim Plateau Volcanics|43595|6|Mentioned|p550||Cambrian|||||||
488|Antrim Plateau Volcanics|43606|6|Mentioned|p5|||||||||
488|Antrim Plateau Volcanics|43652|6|Mentioned|p386||Cambrian|||||||
488|Antrim Plateau Volcanics|43661|6|Mentioned|p2||Cambrian|||||||
488|Antrim Plateau Volcanics|43666|6|Mentioned|p7||Early Cambrian|||||||
488|Antrim Plateau Volcanics|43819|6|Mentioned|p31||Early Cambrian|||||||
488|Antrim Plateau Volcanics|43832|4|Described|30, Table7 p27.||Early Cambrian|Intertongues with Jindare Formation||||||
488|Antrim Plateau Volcanics|43853|5|Briefly described|Map Legend||Early Cambrian|Ord and Bonaparte Basins||||||
488|Antrim Plateau Volcanics|43855|5|Briefly described|Map Legend||Early Cambrian|||||||
488|Antrim Plateau Volcanics|44112|6|Mentioned|p67,78|||||||||
488|Antrim Plateau Volcanics|44113|5|Briefly described|p240|Early Cambrian|Early Cambrian|Geological Province: Daly River Basin||||||
488|Antrim Plateau Volcanics|44133|6|Mentioned|p40|||||||||
488|Antrim Plateau Volcanics|44140|6|Mentioned|p299|Early Cambrian|Early Cambrian|||||||07-MAR-18
488|Antrim Plateau Volcanics|44155|6|Mentioned|p237, p254 Fig.3-40|Cambrian|Cambrian|Less iron-rich than basalts of Halls Creek Group in the same region.|600 Ma.|||||
488|Antrim Plateau Volcanics|44201|14|Not recorded|p.10|||||||||
488|Antrim Plateau Volcanics|44230|5|Briefly described|Map Legend||Early Cambrian|||||||
488|Antrim Plateau Volcanics|44231|5|Briefly described|Map Legend|Cambrian|Cambrian|Dark grey, vesicular and amygdaloidal basalt; may be deeply weathered. Geological Province: Ord Basin.||||||18-MAY-05
488|Antrim Plateau Volcanics|44317|4|Described|Table 4||Cambrian|||||||
488|Antrim Plateau Volcanics|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
488|Antrim Plateau Volcanics|44324|14|Not recorded|p.11||Cambrian|Tb.4 Fig.2.||||||
488|Antrim Plateau Volcanics|44325|14|Not recorded|map legend||Early Cambrian|L.Camb.||||||
488|Antrim Plateau Volcanics|44332|14|Not recorded|p.10,opp.6,map|||(D53-14).||||||
488|Antrim Plateau Volcanics|44333|14|Not recorded|map legend|||Lower Cambrian?||||||
488|Antrim Plateau Volcanics|44363|5|Briefly described|p.19,20,27,29||Early Cambrian|Lower Cambrian.||||||
488|Antrim Plateau Volcanics|44364|14|Not recorded|map legend|||||||||
488|Antrim Plateau Volcanics|44397|14|Not recorded|p.10,13,15,20,Tb.4|||L.Camb.(?)||||||
488|Antrim Plateau Volcanics|44398|14|Not recorded|map legend|||Lower Cambrian (?)||||||
488|Antrim Plateau Volcanics|44411|14|Not recorded|map legend||Early Cambrian|Lower Cambrian.||||||
488|Antrim Plateau Volcanics|44471|14|Not recorded|p.11,12,opp.p.7, map|||(D53-10).||||||
488|Antrim Plateau Volcanics|44472|5|Briefly described|map legend||Early Cambrian|Amygdaloidal basalt, feldspathic sandstone.||||||02-DEC-04
488|Antrim Plateau Volcanics|44482|14|Not recorded|p.11|||(E53-12).||||||
488|Antrim Plateau Volcanics|44693|5|Briefly described|Map Legend||Cambrian|||||||
488|Antrim Plateau Volcanics|44694|5|Briefly described|Map Legend||Cambrian|||||||
488|Antrim Plateau Volcanics|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
488|Antrim Plateau Volcanics|44965|14|Not recorded|Not recorded|||||||||
488|Antrim Plateau Volcanics|45022|14|Not recorded|p2,245||Cambrian|Name is used on many pages, tables & plates||||||
488|Antrim Plateau Volcanics|45038|14|Not recorded|p.33||Early Cambrian|On many pages. p.11,18,21,24,26,28,30,33,31,127, Plate 3,8,37, fig 9,11,12,14,15,22,23,35,36,39,45,16,17,18,21,71,72, L.Camb.||||||
488|Antrim Plateau Volcanics|45047|6|Mentioned|p30|||||||||
488|Antrim Plateau Volcanics|45048|6|Mentioned|Fig.3|||||||||
488|Antrim Plateau Volcanics|45050|6|Mentioned|p42|||Lower Cambrian. See also P44||||||
488|Antrim Plateau Volcanics|45058|6|Mentioned|p18|||L. Cambrian||||||
488|Antrim Plateau Volcanics|45063|6|Mentioned|Fig. 2|||Cambrian. See also Appendix 2||||||
488|Antrim Plateau Volcanics|45064|3|Fully described|Table 1|||See p15||||||18-JUL-06
488|Antrim Plateau Volcanics|45079|6|Mentioned|p39|||Lower Cambrian age||||||
488|Antrim Plateau Volcanics|45087|5|Briefly described|p133|||Chemical analyses.||||||
488|Antrim Plateau Volcanics|45112|5|Briefly described|Table 5|||||||||
488|Antrim Plateau Volcanics|45140|3|Fully described|p13-14,p18,p21,p23, p39-40, p42, p53-54|Early Cambrian|Early Cambrian|See also p60-62, p65, p67-70, p75, p81, p83, Appx.p41-42. Traves (1955); Bultitude (1976). Named after the Great Antrim Plateau, east Kimberley region. Overlies Kimberley and Victoria River regions, Halls Creek Province, Birrindudu Basin and The Granites-Tanami Block. No type section yet defined. 30-1500m thick. Forms broad low rises capped by pisolitic laterite, or mesas and buttes. Locally associated with minor Cu mineralisation; barite in cross-cutting veins. Weathers to heavy grey clay soil. Local source of borewater.||||Unconformably overlies Nongra and Helena Creek Beds, Supplejack Downs Sandstone, Winnecke Granophyre, Tanami Complex, Birrindudu and Limbunya Groups. Underlies Pedestal and Larranganni Beds.|Tholeiitic basalt lavas; minor intercalated chert (commonly stromatolitic) and sandstone (tuffaceous or lithic arenite/greywacke). Most basalt is lateritised, non-porphyritic, sub-aerial; amygdaloidal and vesicular varieties common.|
488|Antrim Plateau Volcanics|45148|4|Described|p8|||Also mentioned p23.||||||18-JUL-06
488|Antrim Plateau Volcanics|45149|6|Mentioned|p38|||See also Table 1 and P15.||||||
488|Antrim Plateau Volcanics|45169|6|Mentioned|Fig.A3|||||||||
488|Antrim Plateau Volcanics|46676|14|Not recorded|p.6|||L. Cambrian.||||||
488|Antrim Plateau Volcanics|46679|14|Not recorded|map legend|||Map legend of Katherine, 1 mile. (D53-9).||||||
488|Antrim Plateau Volcanics|46792|6|Mentioned|p53|||Re stratigraphy||||||
488|Antrim Plateau Volcanics|46844|6|Mentioned|p134|||||||||
488|Antrim Plateau Volcanics|46864|5|Briefly described|p38|||||||||
488|Antrim Plateau Volcanics|47040|6|Mentioned|Fig.3|||||||||
488|Antrim Plateau Volcanics|48635|14|Not recorded|Fig.1||Early Cambrian|(D/52-14). Lower Cambrian.||||||
488|Antrim Plateau Volcanics|48867|14|Not recorded|p.7|||map.||||||
488|Antrim Plateau Volcanics|48886|4|Described|p.35||Early Cambrian|See also Figs + pl.2, App.4, p.78. Lower Cambrian.||||||18-JUL-06
488|Antrim Plateau Volcanics|48927|3|Fully described|p35|||||||||
488|Antrim Plateau Volcanics|48938|4|Described|p73|||||||||
488|Antrim Plateau Volcanics|48942|3|Fully described|p76|||||||||
488|Antrim Plateau Volcanics|48943|3|Fully described|p88|||Structure p105. Strat. section p139.||||||08-JUL-20
488|Antrim Plateau Volcanics|48950|2|Defined|Map legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|49637|5|Briefly described|Fig. 6|Early Cambrian|Early Cambrian|Age: >550Ma.||||||07-FEB-11
488|Antrim Plateau Volcanics|50009|6|Mentioned|p39|Cambrian||||||||
488|Antrim Plateau Volcanics|50085|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|50315|5|Briefly described|Map Legend|Cambrian|Cambrian|Undiff. sediments of sst, siltstone, shale, limestone; basalt lava (white, purple, brown, black), tholeiitic, weathered, generally capped by pisolitic laterite; includes minor volcaniclastic sandstone, lithic arenite and stromatolitic chert. Age: <570Ma.||||||27-OCT-05
488|Antrim Plateau Volcanics|50327|6|Mentioned|p309|||Basaltic volcanics in the interior of the Australia cration.||||||07-FEB-11
488|Antrim Plateau Volcanics|50374|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|50376|5|Briefly described|Map Legend|Cambrian|Cambrian|Age: ~570Ma.||||||19-APR-06
488|Antrim Plateau Volcanics|60006|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Ord Basin. Tholeiitic basalt, sandstone and limestone||||||23-JUL-04
488|Antrim Plateau Volcanics|60283|6|Mentioned|p25 Fig.2|||||||||
488|Antrim Plateau Volcanics|60364|6|Mentioned|p186 Fig.3|||||||||
488|Antrim Plateau Volcanics|60419|5|Briefly described|p1|Early Cambrian|Early Cambrian|Conformably overlain by Goose Hole Group. Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|60519|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Geological Province: Ord Basin. Includes: Bingy Bingy Member, Blackfella Rockhole Member. Basalt and basaltic breccia, sandstone, siltstone and stromatolitic chert.||||||
488|Antrim Plateau Volcanics|60573|5|Briefly described|Map legend|Cambrian|Cambrian|Does NOT outcrop in Roper River mapsheet area.  Basalt: fine to medium-grained, variably altered; composition dominated by plagioclase, clinopyroxene and olivine.||||||23-DEC-09
488|Antrim Plateau Volcanics|60589|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Basalt, sandstone, limestone.  Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|60672|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Porphyritic tholeiitic basalt; laminated red and white chert; tuffaceous sandstone with fragments of chert and vesicular basalt, chert. Unconformably overlies Skull Creek Formation. Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|60676|5|Briefly described|Map legend|Cambrian|Cambrian|Undifferentiated sediments; basalt lava: includes minor volcaniclastic sandstone, lithic arenite and stromatolitic chert.||||||19-JAN-05
488|Antrim Plateau Volcanics|60682|4|Described|piii, 21|Early Cambrian|Early Cambrian|Overlain by Headley Limestone. Tholeiitic flood basalts. Max. thickness: 1000m. Geological Province: Ord Basin.||||||
488|Antrim Plateau Volcanics|60685|3|Fully described|p2 Figure 1, p1|Cambrian|Cambrian|Dominated by flood basalt flows and includes minor interbedded sedimentary and pyroclastic material (sandstone, limestone). Contains at least 7 identifiable lithofacies. Geological Province: Wiso Basin. See also p3 Fig. 2.||||||
488|Antrim Plateau Volcanics|60724|5|Briefly described|p5 Fig. 2|Cambrian|Cambrian|See also p20, p21.||||||
488|Antrim Plateau Volcanics|61023|5|Briefly described|p2 Fig. 2|Precambrian|Precambrian|Geological Province: Bonaparte Basin.||||||10-APR-08
488|Antrim Plateau Volcanics|61272|6|Mentioned|p123|||||||||
488|Antrim Plateau Volcanics|61390|5|Briefly described|Map Legend|Cambrian|Cambrian|Basalt: fine to medium grained, partially altered; composition dominated by plagioclase, clinopyroxene and olivine.||||||23-DEC-09
488|Antrim Plateau Volcanics|61560|5|Briefly described|p497 |Cambrian|Cambrian|Basalts of the Kalkarinji Continental Flood Basalt Province. ||||||
488|Antrim Plateau Volcanics|61566|6|Mentioned|p623|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|61573|5|Briefly described|p676, p681 Tb. 1|Early Cambrian|Early Cambrian|Basalt, minor sandstone, chert, conglomerate and siltstone. Age for a probable feeder dyke: 513Ma (U-Pb). Max. thickness: 150m. ||||||
488|Antrim Plateau Volcanics|61716|6|Mentioned|p650|Cambrian|Cambrian|Age: 507+/-4Ma (Ar-Ar, Glass 2002).||||||
488|Antrim Plateau Volcanics|61732|5|Briefly described|p38|Early Cambrian|Early Cambrian|Flood basalts.  Age: 513+/-12Ma.||||||07-FEB-11
488|Antrim Plateau Volcanics|61826|5|Briefly described|p151, p152, p153|Cambrian|Cambrian|Tholeiitic basalt, minor tuffaceous sandstone, arenite and stromatolitic chert. Geological Province: Birindudu Basin.||||||05-JUN-06
488|Antrim Plateau Volcanics|61861|5|Briefly described|pp4-5, p10, p15, Map 1|Cambrian|Neoproterozoic|||||Unconformably overlies Dead Bullock Formation.|Extensive tholeiitic basalt lava flows with minor sedimentary rocks.|03-APR-12
488|Antrim Plateau Volcanics|62428|5|Briefly described|p351 Tb. 6|Early Cambrian|Early Cambrian|Palaeomagnetic data.||||||10-FEB-09
488|Antrim Plateau Volcanics|62557|4|Described|p461-463|Middle Cambrian|Middle Cambrian|Of the Kalkarindji continental flood basalt province. Ar/Ar age 505+/-2 Ma. Lava flows of mostly aphanitic massive basalt with vesicular or brecciated flow tops. Plagioclase-phyric porphyritic basalt less common. Typically 20-60m thick, up to 200m thick.| Ar/Ar age 505+/-2 Ma.||||Lava flows of mostly aphanitic massive basalt with vesicular or brecciated flow tops. Plagioclase-phyric porphyritic basalt less common.|24-NOV-09
488|Antrim Plateau Volcanics|62580|6|Mentioned|p64|Paleozoic|Paleozoic|In Tanami region.||||||07-FEB-11
488|Antrim Plateau Volcanics|62628|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Murraba Basin. Basalt lava: weathered, tholeiitic, generally capped by ferricrete.||||||
488|Antrim Plateau Volcanics|62869|6|Mentioned|p631 Fig. 6|||||||||
488|Antrim Plateau Volcanics|63022|5|Briefly described|p1013|Cambrian|Cambrian|Belongs to the Kalkarinji large igneous province. Age: 513/-12Ma (from feeder dyke). ||||||
488|Antrim Plateau Volcanics|63062|6|Mentioned|p14|Early Cambrian|Early Cambrian|Flood basalts. Covered broad areas of northern Australia to the SW of Arafura Basin.||||||07-FEB-11
488|Antrim Plateau Volcanics|63458|6|Mentioned|p897 Fig.19. |Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|63762|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|||||||07-FEB-11
488|Antrim Plateau Volcanics|63866|5|Briefly described|p108, p111, p115|Cambrian|Cambrian|Daly Basin. Overlies the Proterozoic stratigraphy in this province.||||||
488|Antrim Plateau Volcanics|64068|5|Briefly described|p81|Early Cambrian|Early Cambrian|Kalkarindji Flood Basalt Province, central and northwest Georgina Basin. c.513-c.504 Ma. ||||||
488|Antrim Plateau Volcanics|64104|6|Mentioned|p75, p76 fig 10|Cambrian|Cambrian|||||||
488|Antrim Plateau Volcanics|64443|6|Mentioned|p7|Cambrian|Cambrian|Dated at 504 +/- 2 Ma (Glass and Phillips, 2002); a probable feeder dyke to these volcanics has been dated at 513 +/- 12 Ma (Hanley and Wingate 2000); typically overlain by Middle Cambrian (Ordian) rocks.||||||
488|Antrim Plateau Volcanics|64571|5|Briefly described|p823, p830, p837|||Age: 513+/-12Ma. Extensive flood basalts. Stratigraphic age is Early to Middle Cambrian, while K/Ar datings yields ages ranging from Early Cambrian to Early Devonian (Bultitude 1972, 1976).||||||16-JUL-13
488|Antrim Plateau Volcanics|64580|4|Described|map legend|Middle Cambrian|Middle Cambrian|Vesicular, amygdaloidal and porphyritic basalt, conglomerate, sandstone; minor interbedded agglomerate, tuff, siltstone, and stromatolitic and laminated chert.||||||16-JUL-13
488|Antrim Plateau Volcanics|64675|6|Mentioned|p10, Fig.19, Fig.21, p21, Map 1|Paleozoic|Neoproterozoic|||||||19-MAR-14
488|Antrim Plateau Volcanics|64784|6|Mentioned|p2,3,6,8 Figs.2-6|Cambrian|Cambrian|Beetaloo Basin.||||Overlies Bukalara Sandstone. Is overlain by Top Springs Limestone.||
488|Antrim Plateau Volcanics|64956|6|Mentioned|p62|Early Cambrian|Early Cambrian|Overlie Soldiers Creek Granite.||||||07-FEB-11
488|Antrim Plateau Volcanics|65074|5|Briefly described|p350-351 figs. 4-36,-37; p358|Early Cambrian|Early Cambrian|See also p359 fig 4-13, p360, p362. Of Birrindudu, Ord, Bonaparte, Wiso and Daly River Basins: widespread outpouring of flood basalts. Type section redefined by Mory and Beere (1985) as the Spring Creek area in the Ord Basin. Thickness from 30m to 1100m.||||Correlated with Table Hill Volcanics of the Officer Basin.|Tholeiitic basaltic lavas and subordinate intercalated chert and sandstone; deeply weathered; amygdaloidal and vesicular varieties also common.|
488|Antrim Plateau Volcanics|65102|6|Mentioned|p373|Early Cambrian|Early Cambrian|Petrographically similar to Kulyong and Table Hill Volcanics, Officer Basin. ||||||
488|Antrim Plateau Volcanics|65194|5|Briefly described|p85|Cambrian|Cambrian|See also reference to superseded name Antrim Plateau Basalts, p12. Lava flows buried alluvial sediments in palaeovalleys in the Tanami-Granites region. Sub-aerial or submarine lava flows, commonly intercalated with shallow marine sedimentary rocks.||||||
488|Antrim Plateau Volcanics|65323|5|Briefly described|Map legend|Cambrian|Cambrian|Non-magnetic sandstone, siltstone and shale (not present on map) and moderately magnetic basalt||||||02-FEB-10
488|Antrim Plateau Volcanics|65324|5|Briefly described|Map legend|Cambrian|Cambrian|Basalt lava: white, purple, brown, black, tholeiitic, weathered, generally capped by pisolitic laterite and includes minor volcaniclastic sst, arenite and chert. Undifferentiated sediments: sst, siltstone, shale, limestone (not shown on map)||||||02-MAR-10
488|Antrim Plateau Volcanics|65326|5|Briefly described|Map legend|Cambrian|Cambrian|Non-magnetic sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt||||||02-FEB-10
488|Antrim Plateau Volcanics|65327|5|Briefly described|Map legend|Cambrian|Cambrian|Not shown on map||||||02-FEB-10
488|Antrim Plateau Volcanics|65328|5|Briefly described|Map legend|Cambrian|Cambrian|Non-magnetic sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt||||||12-APR-10
488|Antrim Plateau Volcanics|65331|5|Briefly described|Map legend + overview geology map legend|Cambrian|Cambrian|Of Ord Basin. Tholeiitic basalt, sandstone, limestone||||||
488|Antrim Plateau Volcanics|65337|4|Described|p61, pp94-95.|Early Cambrian|Early Cambrian|Age of a probable feeder dyke for this unit (Hanley and Wingate 2000). Correlative with Helen Springs Volcanics and others, this constituted a continent-scale flood basalt event. Maximum thickness 1100 m adjacent to Ord Basin, WA.|513 +/- 12, 504 +/- 2 Ma (Glass & Phillips 2002).|Unit in Kalkarindji Volcanic Group.|Includes Malley Spring, Mount Close Chert, Bingy Bingy Basalt and Blackfella Rockhole Members.|||
488|Antrim Plateau Volcanics|65340|5|Briefly described|p63.|Early Cambrian|Early Cambrian||513 +/- 12 Ma (Hanley and Wingate 2000).|||Overlies Bukalara Sandstone.||
488|Antrim Plateau Volcanics|65342|5|Briefly described|p12. |||Daly Basin. Max. thickness at least 106 m. Seen as having potential as an insulating layer for geothermal energy.|||||20-60 m thick basalt flows.|
488|Antrim Plateau Volcanics|65345|6|Mentioned|p3.|||||||||
488|Antrim Plateau Volcanics|65349|5|Briefly described|Map legend|Cambrian|Cambrian|Basalt lava: white, purple, brown, black, tholeiitic, weathered, generally capped by pisolitic laterite and includes minor volcaniclastic sst, arenite and chert. Undifferentiated sediments: sst, siltstone, shale, limestone (not shown on map)||||||02-MAR-10
488|Antrim Plateau Volcanics|65350|6|Mentioned|Map legend|Cambrian|Cambrian|Not shown on map||||||
488|Antrim Plateau Volcanics|65351|5|Briefly described|Map legend|Cambrian|Cambrian|Basalt lava: white, purple, brown, black, tholeiitic, weathered, generally capped by pisolitic laterite and includes minor volcaniclastic sst, arenite and chert. Undifferentiated sediments: sst, siltstone, shale, limestone (not shown on map)||||||02-MAR-10
488|Antrim Plateau Volcanics|65352|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt; non-magnetic||||||
488|Antrim Plateau Volcanics|65353|5|Briefly described|Map legend|Cambrian|Cambrian|Not shown on map||||||12-APR-10
488|Antrim Plateau Volcanics|65354|5|Briefly described|Map legend|Cambrian|Cambrian|Non-magnetic sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt||||||
488|Antrim Plateau Volcanics|65355|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt; non-magnetic||||||02-FEB-10
488|Antrim Plateau Volcanics|65356|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, siltstone and shale (not shown on map) and moderately magnetic basalt; non-magnetic||||||
488|Antrim Plateau Volcanics|65410|6|Mentioned|p74.|||Equivalent to the southern Australian Table Hill Volcanics.||||||
488|Antrim Plateau Volcanics|65416|6|Mentioned|p144.|||Correlated with Table Hill Volcanics (Officer Basin).||||||
488|Antrim Plateau Volcanics|65417|6|Mentioned|p158 Fig.2, p164 Fig.7, p165.|||A major period of strike-slip faulting occurred after the Duerdin Group (c.650 Ma) and before this unit.||||||
488|Antrim Plateau Volcanics|66187|6|Mentioned|p418|Cambrian|Cambrian|Basalts. Occurs in the Petrel Sub-basin of the West Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|67151|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province. Shown with three separately-mapped members, only one of which - Blackfella Rockhole Member - is named.|||Includes Blackfella Rockhole Member.|Unconformably overlies Kinevans Sandstone and Duerdin Group.|Massive and porphyritic tholeiitic basalt.|
488|Antrim Plateau Volcanics|67167|5|Briefly described|Map legend.|Cambrian|Cambrian||||||Basalt, massive and porphyritic, columnar-jointed, sometimes vesicular, with interlayered micaceous siltstone or mudstone.|
488|Antrim Plateau Volcanics|67168|5|Briefly described|Map legend.|Cambrian|Cambrian|||||Unconformably overlies Redcliff Pound, Birrindudu, Mount Winnecke, Tanami and MacFarlane Peak Groups; and Coomarie and Winnecke Suites.|Basalt; sandstone, siltstone, shale.|
488|Antrim Plateau Volcanics|67186|5|Briefly described|Map legend.|Cambrian|Cambrian||||||Basalt, massive and porphyritic, columnar-jointed, sometimes vesicular, with interlayered micaceous siltstone or mudstone.|23-NOV-11
488|Antrim Plateau Volcanics|67269|5|Briefly described|p20-21 Fig.19|Cambrian|Cambrian|East Kimberley. Contains Conophyton basalticum stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).|513 +/- 12 Ma.|||||
488|Antrim Plateau Volcanics|67352|6|Mentioned|p31-32|||Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km.||||||
488|Antrim Plateau Volcanics|67354|6|Mentioned|p89.|||Mentioned as the likely, but not proven, source of volcanics reported from Sunbird-1 in the Kuriyippi Formation.||||||
488|Antrim Plateau Volcanics|67484|6|Mentioned|p294|Cambrian|Cambrian|Mount Ramsay area, West Kimberley and East Kimberley.||||Overlies Louisa Downs and Albert Edward Groups.||
488|Antrim Plateau Volcanics|67620|5|Briefly described|p2-3, 5|Cambrian|Cambrian|May represent the Ediacaran-Cambrian transition.|513 +/- 12 Ma (U-Pb; Hanley and Wingate, 2000).|||Overlies Louisa Downs, Albert Edward, Hawker Groups, and Arumbera Sandstone.||
488|Antrim Plateau Volcanics|67860|4|Described|p416 Fig.4-84, p417, p420 Tb. 4-18, p421|Early Cambrian|Early Cambrian|0-1100 m thick. Type section details given.|||Includes Malley Spring, Mount Close Chert, Bingy Bingy Basalt, and Blackfella Rockhole, Members.|Is overlain by Goose Hole Group.|Vesicular, amygdaloidal and porphyritic basalts; minor agglomerate, tuff, sandstone, siltstone, chert.|
488|Antrim Plateau Volcanics|68138|6|Mentioned|p154|Neoproterozoic|Neoproterozoic|||||||
488|Antrim Plateau Volcanics|68244|6|Mentioned|p663-664,667, p669|Cambrian|Cambrian|||||Underlain unconformably by Louisa Downs Group and Albert Edward Group.||21-JUN-19
488|Antrim Plateau Volcanics|68473|6|Mentioned|p530-533|Cambrian|Cambrian|Mount Ramsay.||||||
488|Antrim Plateau Volcanics|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut.csv|Middle Cambrian|Middle Cambrian|||||Overlies Lally Conglomerate.|Vesicular, amydaloidal and porphyritic basalt, conglomerate, sandstone; minor interbedded agglomerate, tuff, siltstone, and stromatolitic and laminated chert.|
488|Antrim Plateau Volcanics|69018|6|Mentioned|p450 Fig.1b|||||||||
488|Antrim Plateau Volcanics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian|Cambrian|Ord Basin; Southern Bonaparte Basin. Grouped as Antrim Plateau Volcanics and Lally Conglomerate.|||Includes Bingy Bingy Basalt Member, Blackfella Rockhole Member, unnamed quartz sandstone member.||vesicular, amygdaloidal, and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone, limestone, and stromatolitic and laminated chert.|
488|Antrim Plateau Volcanics|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||||Includes Bingy Bingy Basalt Member, Blackfella Rockhole Member||Vesicular, amygdaloidal, and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone and stromatolitic laminated chert.|
488|Antrim Plateau Volcanics|69418|6|Mentioned|p3:29-31, 34|||Kalkarindji Province. Contains barite veins, eg ten deposits at Dorisvale (also known as Pony Pocket) and six veins in the Inverway area (described). Also contains widely distributed prehnite, eg at the Sun Jade deposit.||||||12-JUL-16
488|Antrim Plateau Volcanics|69420|6|Mentioned|p5:117|||Kalkarindji Province. Mentioned as a possible source of base metals in the Wonarah phosphate deposit in the Georgina Basin.||||||12-JUL-16
488|Antrim Plateau Volcanics|69426|6|Mentioned|p11:9-10|||||||Unconformably overlies Mount Charles Formation.|Basalt.|12-JUL-16
488|Antrim Plateau Volcanics|69429|6|Mentioned|p14:2 Fig.14.2|Early Cambrian|Early Cambrian|||||||12-JUL-16
488|Antrim Plateau Volcanics|69430|5|Briefly described|p15:29-30, 62-63|Cambrian|Cambrian|Primary bitumen has been discovered in a sedimentary interval within this unit, indicating active generation or remigration from Mesoproterozoic source rocks (Roper Group).||||Unconformably overlies Bukalara Sandstone. Is overlain by Top Springs Limestone.||12-JUL-16
488|Antrim Plateau Volcanics|69432|6|Mentioned|p17:13-14|Early Cambrian|Early Cambrian|Kalkarindji Province. Mentioned in the context that the Limbunya Fault and others (in the Birrindudu Basin) were reactivated after extrusion of this unit and deposition of Cambrian sediments. Hosts non-economic barite prospects.||||||12-JUL-16
488|Antrim Plateau Volcanics|69437|6|Mentioned|p22:10, 14|Series 3|Series 2|Kalkarindji Large Igneous Province. Contains widespread but economically insignificant Cu mineralisation.||||||12-JUL-16
488|Antrim Plateau Volcanics|69440|6|Mentioned|p25:1|Early Cambrian|Early Cambrian|||||||12-JUL-16
488|Antrim Plateau Volcanics|69441|6|Mentioned|p26:5|Early Cambrian|Early Cambrian|Some reactivation of faults in the Victoria Basin postdates this unit.||||||12-JUL-16
488|Antrim Plateau Volcanics|69442|6|Mentioned|p27:3 Tb.27.1; 5|||||||Overlies unconformably Uniya Formation.||08-JUL-20
488|Antrim Plateau Volcanics|69445|2|Defined|p30:1-6, 8-12, 16-17|Early Cambrian|Early Cambrian|Traves (1955). Formerly Antrim Plateau Basalts of David (1932); subsequently Antrim Plateau Basalt (McLeod, 1965), Antrim Volcanics (Beattie and Brown, 1984). First described by Hardman (1885) and Jensen (1915). Widespread sub-aerial basaltic lavas. Included in Kalkarinji (later Kalkarindji) Continental Flood Basalt Province by Glass et al. (2006), Glass and Phillips (2006). In this article this unit is part of the Kalkarindji Suite (new name). Synonymous with Nutwood Downs Volcanics. Type section is Spring Creek in DIXON RANGE map area, where it is 1000m thick: grid co-ordinates in Mory and Beere (1985) p38; (1988) p10. Up to 1100m thick. Age determinations include Ar40/Ar39 plagioclase separates: 508 +/- 2 Ma and 505 +/- 2 Ma (average 507 +/- 2 Ma) by Glass and Phillips (2006). Is overlain unconformably by Headleys, Montejinni and Tindall Limestones. Is displaced by the Neave, Negri, Blackfella Creek and West Baines Faults. Associated with widespread but economically insignificant Cu mineralisation, near and along the contact with Headleys Limestone. Contains very thin bitumen seams, as well as gemstones and semi-precious minerals (amethyst, prehnite, agate).|507 +/- 2 Ma.|Kalkarindji Suite.|Bingy Bingy Basalt, Blackfella Rockhole, Malley Spring, Mount Close Chert, Members.|Overlies Lally Conglomerate and, unconformably, the Wattie, Bullita, Tijunna, Auvergne, Albert Edward Groups; Mount Forster Sandstone, Moonlight Valley Tillite and Bukalara Sandstone.|Predominantly basaltic lava flows, minor flow breccia and agglomerate, and (in WA) dolerite dykes; local thin (<10m) interbeds of well-sorted cross-bedded sandstone, siltstone, chert, sedimentary breccia and silicified stromatolites (Conophyton sp).|12-JUL-16
488|Antrim Plateau Volcanics|69446|5|Briefly described|p31:1-2, 9, 11|Early Cambrian|Early Cambrian|Part of the basement to Daly Basin. Associated with economically insignificant base metal (esp. copper) occurrences along the upper contact.||||Is overlain unconformably by Tindall Limestone.||12-JUL-16
488|Antrim Plateau Volcanics|69447|5|Briefly described|p32:1-2, 8|Early Cambrian|Early Cambrian|Kalkarindji Province. Forms part of the basement for the Wiso Basin. Associated with economically insignificant copper occurrences at its upper contacts, particularly with Montejinni Limestone (eg Crowsons Prospect).||||||12-JUL-16
488|Antrim Plateau Volcanics|69448|5|Briefly described|p33:1-5, 8|Early Cambrian|Early Cambrian|Part of the basement to the Ord Basin. Has undergone ferruginisation and silicification, either by weathering prior to burial or by more recent processes. Displaced by the NW-trending Negri Fault. Associated with widespread but mostly economically insignificant copper occurrences.||||Is overlain disconformably by Headleys Limestone or (locally) unconformably by Nelson Shale.||12-JUL-16
488|Antrim Plateau Volcanics|69451|6|Mentioned|p35:7|||||||||12-JUL-16
488|Antrim Plateau Volcanics|69452|5|Briefly described|p36:5, 10|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Is overlain unconformably by Carlton Group.|Tholeiitic basalts.|12-JUL-16
488|Antrim Plateau Volcanics|69453|5|Briefly described|p37:1|Cambrian|Cambrian|Kalkarindji Province.||||Is overlain unconformably by Pedestal beds.||12-JUL-16
488|Antrim Plateau Volcanics|69458|5|Briefly described|p42:20|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Is overlain unconformably by Camfield beds.||14-SEP-18
488|Antrim Plateau Volcanics|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Tindall Limestone, Jindare Formation||
488|Antrim Plateau Volcanics|69587|5|Briefly described|500k_geologyp08_lut.csv|Middle Cambrian|Middle Cambrian||||||Vesicular, amydaloidal and porphyritic basalt, conglomerate, sandstone; minor interbedded agglomerate, tuff, siltstone, and stromatolitic and laminated chert|
488|Antrim Plateau Volcanics|69597|5|Briefly described|p2|Cambrian|Cambrian|Ord Basin. |c. 510 Ma|||Unconformably overlain by the Cockatoo Formation.|Mafic volcanic rocks.|
488|Antrim Plateau Volcanics|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin, Southern Bonaparte Basin. Events: Alice Springs Orogeny; Mount Eclipse Movement; Pertnjara-Brewer Movements. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|508-505 Ma (Isotopic)||Includes Bingy Bngy Basalt Member, Blackfella Rockhole Member.|Associated with Lally Conglomerate.|Vesicular, amygdaloidal, and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone, limestone, and localised stromatolitic and laminated chert|
488|Antrim Plateau Volcanics|69673|6|Mentioned|p32, p168 fig 139, p186|||Kalkarindji Province.||||Overlain by Tarrara Formation||
488|Antrim Plateau Volcanics|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_interpgeop_lut.csv.|505-508 Ma||Bingy Bingy Basalt Member, Blackfella Rockhole Member, Lally Conglomerate||Vesicular, amygdaloidal and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone and limestone. Localised stromatilitic chert.|
488|Antrim Plateau Volcanics|70206|5|Briefly described|Map Legend|Cambrian|Cambrian|Kalkarindji Province.|||||Massive porphyritic and tholeiitic basalt.|
488|Antrim Plateau Volcanics|70315|4|Described|p22-p23, p26, p30-p31|||Kalkarindji Province. A semi-continuous outcrop of c. 50 000km^2 with a maximum thickness of 1.1 km. Referred to as the APV throughout the text.|||Includes the Blackfella Rockhole Member, Malley Springs Sandstone Member, Mount Close Chert Member, Bingy Bingy Basalt Member.||Basaltic lava fields, the majority is basaltic tholeiitic pahoehoe flows.|
488|Antrim Plateau Volcanics|70380|5|Briefly described|p745-746|Early Cambrian|Early Cambrian|Kalkarindji Large Igneous Province. Forms basement to Daly, Wiso and northern Georgina Basins.||||||
488|Antrim Plateau Volcanics|70655|5|Briefly described|Map Legend|Cambrian|Cambrian|Kalkarindji Province.|||Includes Blackfella Rockhole Member and 2 un-named units.|Unconformably overlies Kinevans Sandstone, Moonlight Valley Tillite, Saddle Creek Formation.|Massive and porphyritic tholeiitic basalt.  Red-brown sandstone. Sandstone, laminated chert. Agglomerate, brecciated flow tops.|
488|Antrim Plateau Volcanics|70731|6|Mentioned|p278|Cambrian|Cambrian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. ||||||
488|Antrim Plateau Volcanics|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Southern Bonaparte Basin.||||||
488|Antrim Plateau Volcanics|70848|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||||Basalt lava: weathered, tholeiitic, generally capped by ferricrete, contains minor sandstone, chert.|
488|Antrim Plateau Volcanics|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province. The two facies are mapped separately.|||||Mainly massive porphyritic and tholeiitic basalt; also friable cross-bedded quartz sandstone with some surface silicification.|
488|Antrim Plateau Volcanics|70851|5|Briefly described|p7, p16-p19, p29, p34|Cambrian|Cambrian|Eastern Zone, Lamboo Province. Belongs to the Kalkarindji Large Igneous Province. Geophysical response is discussed. Interpreted to be overlain by the Cockatoo Group.|c. 510 Ma|||Overlies the Carr Boyd and Duerdin groups.||28-MAR-23
488|Antrim Plateau Volcanics|70852|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||||Basalt lava: weathered, tholeiitic, generally capped by ferricrete, contains minor sandstone, chert.|
488|Antrim Plateau Volcanics|70854|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.||||Unconformably overlies Auvergne Group. Overlies the Skull Creek and Timber Creek Formations.|Porphyritic tholeiitic basalt. Occurrences of laminated red and white chert, and tuffaceous sandstone with fragments of chert and vesicular basalt, are mapped separately.|21-SEP-17
488|Antrim Plateau Volcanics|70855|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.||||Unconformably overlies Tijunna Group and (locally) Bullita Group.|Massive porphyritic and tholeiitic basalt. Three facies are mapped separately: agglomerate; friable cross-bedded quartz sandstone with some surface silicification; laminated chert, stromatolitic in part.|
488|Antrim Plateau Volcanics|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|505 +/- 2 Ma.|Kalkarindji Suite.|||Basalt, massive and porphyritic, locally columnar-jointed, sometimes vesicular, with interlayered micaceous siltstone and mudstone.|
488|Antrim Plateau Volcanics|70968|5|Briefly described|p75, p84|Early Cambrian|Early Cambrian|Fence diagram of wells in Beetaloo Sub-basin.||||Unconformably overlies Chambers River Formation, Hayfield mudstone and Bukalara Sandstone.||
488|Antrim Plateau Volcanics|71080|6|Mentioned|p7, p37|Cambrian|Cambrian||c. 510 Ma|||Unconformably overlies Erica Formation, Redcliff Pound Group in NT.||
488|Antrim Plateau Volcanics|71146|5|Briefly described|p6, p9, p18, p21, p22, p45|Cambrian|Cambrian|Ord Basin, Kalkarindji Large Igneous Province.|509 +/- 2.2 Ma |||Unconformably overlies the Albert Edward and Louisa Downs Groups. Overlain by the Tararra Formation (Carlton Group) and the Negri Subgroup.|Volcanics.|
488|Antrim Plateau Volcanics|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin; Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|508+\-2 to 505+\-2 Ma (isotopic)|Unit of Kalkarindji Suite.|Includes Bingy Bingy Basalt Member, Blackfella Rockhole Member.||Vesicular, amygdaloidal, and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone, limestone, and localised stromatolitic and laminated chert|
488|Antrim Plateau Volcanics|71369|6|Mentioned|p45|Cambrian|Cambrian|||||Correlative of Colless Volcanics.||
488|Antrim Plateau Volcanics|71374|5|Briefly described|p21|Cambrian|Cambrian|||||Unconformably overlies the Chambers River Formation.||
488|Antrim Plateau Volcanics|71632|5|Briefly described|Map legend.|||Daly, Georgina Basins. Widespread. Mapped as one unit with Daly River Group and Jindare Formation, and as another unit with Bukalara Sandstone, Cox Formation, Nutwood Downs Volcanics and Top Springs Limestone.||||||
488|Antrim Plateau Volcanics|71754|14|Not recorded|p195|||||||||
488|Antrim Plateau Volcanics|71784|6|Mentioned|p85-86|||||||||
488|Antrim Plateau Volcanics|71800|5|Briefly described|p25-p26|||Ord Basin.|c. 513-505 Ma|||Conformably overlain by the Goose Hole Group.||
488|Antrim Plateau Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Series 3|Series 3|Ord Basin; Southern Bonaparte Basin, Halls Creek Orogen.|508 +/-2 Ma max, 505+/-2 Ma min||||Vesicular, amygdaloidal, and porphyritic basalt and basaltic breccia; minor interbedded conglomerate, sandstone, siltstone, limestone, and localised stromatolitic and laminated chert.|
488|Antrim Plateau Volcanics|72437|5|Briefly described|p14, p130|Cambrian|Neoproterozoic|Described by Roberts et al (1965; 1968) and Bultitude (1971). One whole rock analysis is presented.|||||Extensive flood basalts.|
488|Antrim Plateau Volcanics|72490|5|Briefly described|p3-4|||Part of the c. 511 Ma Kalkarindji large igneous province.||Kalkarindji Supersuite|||Massive and amygdaloidal tholeiitic basalt and basalt breccia; commonly capped by ferricrete. Agglomerate with brecciated flow tops. Minor sandstone and chert interbeds.|
488|Antrim Plateau Volcanics|72718|6|Mentioned|p7, p10|||Southern McArthur Basin. Urapunga Fault Zone and southwestern McArthur Basin. Strongly disrupts seismic signals.||||Underlain[?] by Bukalara Sandstone.||
488|Antrim Plateau Volcanics|73083|6|Mentioned|p3|Cambrian|Cambrian|[Superseded by or a constituent of the Kalkarindji Suite]. These rocks comprise one of a series of widely separated exposures of Cambrian basalt attributed to the Kalkarindji Continental Flood Basalt Province (Glass et al, 2013). Correlation was based on matching magnetic signatures.|||||Basalt.|
488|Antrim Plateau Volcanics|73089|6|Mentioned|p9, p43|Cambrian|Cambrian|Part of the Kalkarindji Large Igneous Province [c. 508 - 498 Ma Ar-Ar date for LIP?]. May be linked to the apparent 600-400 Ma Pb loss of zircon from units in the area.|510-500 Ma||||Mafic volcanic rocks and subordinate siliciclastic sedimentary rocks.|
488|Antrim Plateau Volcanics|73445|5|Briefly described|p5|Cambrian|Cambrian|Preserves some palaeovalleys in the Granites-Tanami region.||||||
524|Aralka Formation|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
524|Aralka Formation|22561|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22566|6|Mentioned|p81|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
524|Aralka Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22648|6|Mentioned|p 127|||||||||
524|Aralka Formation|22649|4|Described|p 153|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22651|6|Mentioned|Fig 11 btw p182-183|Proterozoic|Proterozoic|||||||
524|Aralka Formation|22762|5|Briefly described|p362|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22804|5|Briefly described|p443|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Geol. Prov: Amadeus Basin||||||18-JUL-06
524|Aralka Formation|22826|6|Mentioned|p569|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Correlate of Etina Formation, Sunderland Formation and Tapley Hill Formation (Umberatana Group) and Brighton Limestone and Angepena Formation equivalent.||||||
524|Aralka Formation|23314|5|Briefly described|331 Fig.2|||||||||
524|Aralka Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|Age: ~650Ma||||||18-JUL-06
524|Aralka Formation|23361|5|Briefly described|16 Fig.4|Cryogenian|Cryogenian|||||||
524|Aralka Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|24301|6|Mentioned|p16|||||||||
524|Aralka Formation|35805|6|Mentioned|Fig.3|||||||||
524|Aralka Formation|35863|6|Mentioned|Table 1|||||||||
524|Aralka Formation|36898|6|Mentioned|Fig.4|||||||||
524|Aralka Formation|37462|4|Described|Table 4.IX|||||||||
524|Aralka Formation|37928|6|Mentioned|p517|||||||||
524|Aralka Formation|37929|6|Mentioned|Fig.2|||||||||
524|Aralka Formation|38157|6|Mentioned|Table VI|||||||||
524|Aralka Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|39565|6|Mentioned|p31|||||||||
524|Aralka Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Laminated grey-green to red-brown siltstone and shale with beds of limestone, some oolitic or stromatolitic. Geological Province: Amadeus Basin.||||||14-FEB-06
524|Aralka Formation|40105|6|Mentioned|p311|||||||||
524|Aralka Formation|40740|4|Described|p12|||||||||
524|Aralka Formation|40852|6|Mentioned|p29|||||||||
524|Aralka Formation|40906|6|Mentioned|Fig.9|||||||||
524|Aralka Formation|41005|6|Mentioned|Fig.2|||||||||
524|Aralka Formation|41039|6|Mentioned|Fig.2|||||||||
524|Aralka Formation|41190|6|Mentioned|Fig.4|||||||||
524|Aralka Formation|41270|6|Mentioned|Table 1|||||||||
524|Aralka Formation|41405|6|Mentioned|p205|||||||||
524|Aralka Formation|41618|6|Mentioned|Fig.2|||||||||
524|Aralka Formation|41717|6|Mentioned|Fig.2|||||||||
524|Aralka Formation|41852|6|Mentioned|p219|||||||||
524|Aralka Formation|42059|5|Briefly described|p130|||See also Fig.2||||||
524|Aralka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
524|Aralka Formation|42082|6|Mentioned|Fig.3 P323|||||||||
524|Aralka Formation|42198|6|Mentioned|p265|||||||||
524|Aralka Formation|42504|4|Described|p72|||||||||
524|Aralka Formation|42643|6|Mentioned|Fig.4 P19|||||||||
524|Aralka Formation|42845|6|Mentioned|p498|||||||||
524|Aralka Formation|42886|6|Mentioned|Fig.2 P219|||||||||
524|Aralka Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Shale. Geological province: Amadeus Basin.||||||23-JAN-08
524|Aralka Formation|43105|5|Briefly described|Fig.3,p8|||||||||
524|Aralka Formation|43503|6|Mentioned|11-50|||age from Ediacaran||||||
524|Aralka Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
524|Aralka Formation|43756|6|Mentioned|p542|||||||||
524|Aralka Formation|44111|6|Mentioned|p.58, Fig. 2|||in Amadeus Basin, presented as "Aralka" only in Fig. 2 on p.58||||||11-JUN-15
524|Aralka Formation|45155|6|Mentioned|Fig.7|||Amadeus Basin||||||
524|Aralka Formation|46865|2|Defined|p52|Adelaidean|Adelaidean|||||||
524|Aralka Formation|46903|6|Mentioned|Fig.5|||Correlation chart||||||
524|Aralka Formation|49796|5|Briefly described|Sect C BDF1 & 32|||Of Olympic Formation or Bitter Springs Formation.||||||18-JUL-06
524|Aralka Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Contains Limbla and Ringwood Members.  Laminated grey-green siltstone and shale with beds of limestone, some oolitic or stromatolitic.||||||02-FEB-05
524|Aralka Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
524|Aralka Formation|61732|5|Briefly described|p4 Fig. 3, p37|Sturtian|Sturtian|Overlies the Areyonga Formation. Geological Province: Amadeus Basin.||||||07-FEB-11
524|Aralka Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||11-FEB-10
524|Aralka Formation|62379|5|Briefly described|p7 Fig. 2, p29|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Pyritic/calcareous siltstone and shale.||||||
524|Aralka Formation|62453|5|Briefly described|p12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Amadeus Basin.||||||
524|Aralka Formation|62903|5|Briefly described|p729, p730, p731|||Amadeus Basin. Depositional environment was intracratonic basin (Preiss 2000). Age for base of Aralka Formation constrains age of underlying Areyonga glacial deposits. Very thin stratigraphic thickness of Aralka Formation preserved in Wallara-1 (~27 m) may be a lacuna unconformity between the Aralka and Olympic Formations. A Three-point Re-Os date of 592+/-14 Ma is challenged (Hoffmann et al. 2004).|657.2+/-5.4 Ma Re-Os|||conformably overlies Areyonga Formation; is overlain by hiatus of unknown duration then Olympic Formation, abrupt contact in drillcore.|dolomitic shales and (organic-rich) siltstones|
524|Aralka Formation|63458|5|Briefly described|p897 Fig.19. |Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Areyonga Formation. Is overlain by Olympic Formation.||11-JUN-15
524|Aralka Formation|63562|5|Briefly described|p338 fig 3, p342, p351, p352 fig 10|Cryogenian|Cryogenian|Of Amadeus Basin. [Different age determinations quoted 664-578 Ma].|658 +/- 6 Ma (Re-Os: Kendall and Creaser, 2004).||Limbla Member.|Overlies Areyonga Formation.|Siliciclastics including tillites, and stromatolitic carbonates.|06-DEC-17
524|Aralka Formation|64625|5|Briefly described|p245 fig 2, p256|||Amadeus Basin. Deep-water sediments.||||Overlies Areyonga Formation. Unconformably overlain by Pioneer Sandstone, Olympic Formation|Dominantly shale.|
524|Aralka Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Cryogenian|Deposited in the Amadeus Basin during the Centralian 2 event (~700-635 Ma)||||||
524|Aralka Formation|64778|6|Mentioned|p13, 16, 18, 21-22, 27|Neoproterozoic|Neoproterozoic|Amadeus Basin. Max. palaeotemperature analysis summary. Potential hydrocarbon source.||||||
524|Aralka Formation|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|||||||
524|Aralka Formation|64797|5|Briefly described|p151, p153 Fig.2, p156-158, p164 Fig.11 |||See also p167 Tb.10, p168 Tb.11, p170, p175. Of Amadeus Basin. S-isotope data.|||Includes Ringwood Member.|Correlated with Tapley Hill Formation (Adelaide Rift Complex). Contacts Areyonga Formation.||
524|Aralka Formation|64809|6|Mentioned|p2, p3 Fig.2, p6 Fig.4, p10 |Proterozoic|Proterozoic|Late Proterozoic||||||
524|Aralka Formation|64970|6|Mentioned|p719 Fig. 2|Sturtian|Sturtian|Geological Province: Amadeus Basin.||||||27-MAY-09
524|Aralka Formation|65233|4|Described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Overlies the Areyonga Formation. Geol.prov: Amadeus Basin. Together with Areyonga Formation, this glaciogenic succession shows marked lithological variation (details included) - black shales of this unit in the NE part of basin are up to 1000m thick.||||||07-FEB-11
524|Aralka Formation|65272|6|Mentioned|p320 Fig.3||Cryogenian|||||||
524|Aralka Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Amadeus Basin||||||
524|Aralka Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Amadeus Basin||||||
524|Aralka Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 2.||||||
524|Aralka Formation|65489|6|Mentioned|p125|Proterozoic|Proterozoic|Amadeus Basin.||||Is overlain by Pertatataka Formation.||
524|Aralka Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|Amadeus Basin. Type area is 6.4 km SE of Ringwood Station homestead. Up to c.1000m thick in the NE of the Basin.||||Conformably overlies Areyonga Formation. Is overlain disconformably by Olympic Formation.|Siltstone, shale, dolostone, sandstone and grainstone.|
524|Aralka Formation|67326|5|Briefly described|p2, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin. Mentioned as a possible alternative (to Pertatataka Formation) source of gas in the Dingo gas field.||||Overlies Areyonga Formation. Is overlain by Olympic Formation.||
524|Aralka Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Areyonga Formation. Is overlain by Olympic Formation.||
524|Aralka Formation|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Amadeus Basin.||||Overlies Areyonga Formation. Is overlain by Olympic Formation.||
524|Aralka Formation|67856|5|Briefly described|p338 fig 4-30, p345 fig 4-34|Neoproterozoic|Neoproterozoic|||||||
524|Aralka Formation|68244|6|Mentioned|p671||Neoproterozoic|Amadeus Basin. Maximum age of 657.2+\-5.4 Ma by Kendall et al., 2006.||||||
524|Aralka Formation|68270|4|Described|p679,683,687|Cryogenian|Cryogenian|Amadeus Basin. Re-Os date of 657.2+\-5.4 Ma for organic-rich (TOC 0.5-1.0%) shales of the lower Aralka Fm. in drill hole Wallara 1 (Kendall et al. 2006), consistent with age from ash bed in the Wilyerpa Formation, and Re-Os dates from post-Sturt glacial shale units that paraconformably overlie diamictites in the Adelaide Rift Complex (643+\-2.4 Ma; Kendall et al. 2006) and NW Tasmania (640.7+\-4.7 Ma; Kendall et al. 2007).||||Overlain disconformably by Pioneer Sandstone and Olympic Formation. Underlain conformably to disconformably by Areyonga Formation.||
524|Aralka Formation|68275|6|Mentioned|p58, 62|||Post-glacial rocks. Associated with the Tapley Hill Formation in that they both show sustained and very high positive 34S (pyrite) isotope anomalies; a unique chronostratigraphic marker.||||||
524|Aralka Formation|68316|6|Mentioned|p778 Fig.1|||||||||
524|Aralka Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
524|Aralka Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
524|Aralka Formation|68733|6|Mentioned|p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.||||Equivalent to Lower Inindia Beds.||04-DEC-17
524|Aralka Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
524|Aralka Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 2.||||Overlies Areyonga Formation. Is overlain by Pioneer Sandstone and Olympic Formation.|Includes sandstone and shale.|12-JUL-16
524|Aralka Formation|69438|3|Fully described|p23:2-5, 7, 16-18, 21, 43, 52-53, 59-60|Cryogenian|Cryogenian|Priess et al. (1978). Originally included in the basal Pertatataka Formation by Wells et al. (1967). Amadeus Basin. Is estimated to be c.1000m thick in the type area in the NE of the Basin. Potentially important petroleum source rock. Age estimates are discussed. Hosts two unnamed Pb-Zn occurrences, and the Waldo Pedlar Bore Cu occurrence. One of the most likely oil- and/or gas-prone units in the Basin. Thick shales seal Areyonga Formation reservoirs.|c.600 Ma.||Ringwood, Limbla Members.|Conformably overlies Areyonga Formation. Is overlain disconformably by Olympic Formation. Is correlated with Tapley Hill Formation and Inindia beds.|Mainly poorly exposed to concealed siltstone and shale; includes a dolostone/limestone Member and a limestone/sandstone Member.|12-JUL-16
524|Aralka Formation|69439|6|Mentioned|p24:7|||Amadeus Basin.||||Correlated with Rinkabeena Shale.||12-JUL-16
524|Aralka Formation|69606|4|Described|p1, p3, p4 fig 2, p5, p6 fig 3|Cryogenian|Cryogenian|Of Supersequence 2. c. 450m thick. Potential source and seal rock in the NT. Amadeus Basin. Sparse outcrop is restricted to siltstone and rarer fine grained sandstone and elsewhere bands of dolostone crop out intermittently. A ridge forming limestone unit marking the top of the formation outcrops in the eastern Boord Ridges and thins out and disappears to the west.  Stromatolites consist of isolated domes ranging from tens of centimetres to over 1 metre; these are rarely intact. Also referred to as the 'upper Aralka Formation' on p12. Unconformably overlain by an unnamed glacigene unit. See also p7 fig 4, p10, p11 fig 6, p12, p13 fig 7, p14, p18, p19.||||Overlies the Areyonga Formation. Unconformably overlain by the Olympic Formation and Pioneer Sandstone.|Siltstone and shale with minor very fine grained sandstone interbeds; stromatolitic and intraclastic dolostone interbeds. Sandy, intraclastic and stromatolitic limestone occurs at the top of this formation.|15-SEP-22
524|Aralka Formation|69673|5|Briefly described|p63, p74, p81, p86, p89, p91, p98|Neoproterozoic|Neoproterozoic|Potential source rock, potential reservoir rock. Maximum thickness of 1km.|||Includes Ringwood Member, Limbla Member|Conformably overlies Areyonga Formation, disconformably overlain by Olympic Formation, correlated with Inindia beds|Sandstone and shale.|
524|Aralka Formation|69937|4|Described|v-vi, p3 Tb.1, p11, p14-16, p43-44|Neoproterozoic|Neoproterozoic|NE and north-central Amadeus Basin. Originally included in the basal part of the Pertatataka Formation by Wells et al. (1967). Likely zircon provenance discussed. Estimated age of c.600 Ma, based on correlations with other glacial successions, is considerably younger than the youngest detrital zircon.|||Ringwood, Limbla Members.|Conformably overlies Areyonga Formation. Is overlain dis- or un-conformably by Olympic Formation.|Siliciclastics and carbonates. Mainly poorly-exposed to concealed siltstone and shale, but with a limestone-dolostone Member and a limestone-sandstone Member.|
524|Aralka Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 2 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin. Re-Os age of 657+\-5.4 Ma at the base of the Aralka Formation (Kendall et al., 2006).||||Overlain by Pioneer Sandstone/Olympic Formation. Underlain by Areyonga Formation.||
524|Aralka Formation|70416|3|Fully described|p62-70, p72, p74, p77, p79-80|Cryogenian|Cryogenian|Preiss et al. (1978). Amadeus Basin; defined in the NE; now recognised across much of the Basin. Has been included inconsistently in earlier definitions of Pertatataka and Areyonga Formations. In S and W Northen Territory, this unit was included in Inindia beds. Contains stromatolites: Tungussia inna, and a new Group and Form: Atilanya fennensis (Systematic palaeontology descriptions). A proven hydrocarbon source (briefly described). Interglacial: post-Sturt and pre-Elatina. Largely recessive; poorly exposed.|657 +/- 5.4 Ma (Re-Os: Kendall et al., 2006).||Ringwood, Limbla Members.|Conformably overlies Areyonga Formation. Is overlain unconformably by Olympic Formation and Pioneer Sandstone. Is correlated with part of Inindia beds.|Siltstones (including stromatolitic siltstone) and shales with minor carbonates (dolostone), sandstones and calcarenite.|
524|Aralka Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Olympic Formation or Pioneer Sandstone. Underlain by Areyonga Formation.||
524|Aralka Formation|71001|5|Briefly described|p18 Fig.2, p19-20, 23, 27|Cryogenian|Cryogenian|Amadeus Basin. Marine deposits. Carbon isotope correlation graph.|||Ringwood, Limbla Members.|Overlies Areyonga Formation. Is overlain by Olympic Formation.|Interglacial black shale.|
524|Aralka Formation|71080|6|Mentioned|p29 fig 20, p30, 31|Cryogenian|Cryogenian|Amadeus Basin. Supersequence 2. Includes gas-prone source-rock characteristics in black shales.|||||Dominantly shale.|
524|Aralka Formation|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
524|Aralka Formation|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
524|Aralka Formation|71344|4|Described|p1094, 1093, 1095, 1096-1103|Cryogenian|Cryogenian|Amadeus Basin. Age from rhenium-osmium dating. Sedimentary features indicate shallowing-upward cycles in a generally shallow marine depositional environment in the lower part and a deltaic environment in the upper part.|~657 Ma (Re-Os: Kendall et al., 2006).|Of Inindia Package.|Includes Ringwood Member, Limbla Member.|Conformably overlies the Areyonga Formation. Unconformably overlain by the Olympic Formation.|Siltstones, shales and dolomites|10-NOV-17
524|Aralka Formation|71801|6|Mentioned|p230, p232, p234-p235, p237|Cryogenian|Cryogenian|Amadeus Basin.|||Includes the Ringwood Member and the Limbla Member.|Overlies the Areyonga Formation. Overlain by the Olympic Formation.||
524|Aralka Formation|71810|5|Briefly described|Map legend.|Cryogenian|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|c.657 Ma.||||Siltstone, shale, limestone, dolomite, and minor sandstone; stromatolitic.|
524|Aralka Formation|71841|5|Briefly described|iii,p1-7,9-12,14|Cryogenian|Cryogenian|Of Amadeus Basin. Original stratigraphy based on McKinnon-Matthews (2009): Not originally recognised in CPD001, 002 and 003. Revised stratigraphy in drill core: CPD001: 0-101m. CPD002: 0-47m. CPD003: 201.1-219m EOH. See p3-4 (CPD001), p6-7 (CPD002), p9-12 (CPD003) for lithological descriptions based on revised drill core intervals.|||Includes Limbla and Ringwood members.|Overlain by Pioneer Sandstone or Olympic Formation. Underlain by Areyonga Formation. Grades into Inindia beds.||19-SEP-19
524|Aralka Formation|71842|5|Briefly described|iii,p1-3,5,7,9|Cryogenian|Cryogenian|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Forms the low-lying area between the prominent ridges of the Mount Conner area.|||Includes Limbla and Ringwood members.|Overlain by Olympic/Pioneer Formation. Underlain by Areyonga Formation. Correlable with Inindia beds.||08-JAN-20
524|Aralka Formation|72369|4|Described|iii,p3-4,7-9,, p15, 44|||Of Amadeus Basin.  Originally of Preiss et al (1978). Exposed in the NE, and to a lesser extent, north-central portion of the Amadeus Basin. Inferred maximum age of c. 600 Ma based on its stratigraphic position above Sturtian glacial succession (Edgoose 2013), supported by Re-Os ages of 658+\-5 Ma (Kendall and Creaser 2004) and 657.2+\-5.4 Ma (Kendall et al 2006) from Wallara-1 well. LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN278 (fine-grained calcareous sandstone) yielded an interpreted maximum depositional age of 844+\-3 Ma (youngest concordant zircon) but does not further constrain the timing of deposition of the unit. Contains significant proportion of detrital zircons derived from Musgrave Province (c. 1205 to c. 1125 Ma spectrum), and Aileron and Warumpi provinces (c. 1800 to c. 1600 Ma age spectrum). A distal source for c. 975 Ma zircons is inferred based on the lack of potential primary sources in proximal regions. Sample locality, zircon description, SHRIMP results and analyses are discussed.|||Includes Limbla and Ringwood members.|Overlain disconformably by Olympic Formation or Winnall Group. Underlain unconformably by Areyonga Formation.|Variably calcareous shale and siltstone.|18-DEC-19
524|Aralka Formation|72375|4|Described|p1-2,19|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Occurs in NE and, to a lesser extent, in the north-central Amadeus Basin. Originally included in the basal part of Pertatataka Formation by Wells et al (1967). Estimated age at c. 600 Ma based on correlations with Neoproterozoic glacial successions.|||Includes Limbla Member, Ringwood Member.|Overlain disconformably by Olympic Formation. Underlain by Areyonga Formation.|Dominated by poorly exposed to concealed siltstone and shales.|
524|Aralka Formation|72489|4|Described|p3, p4 Fig.3, p5 Fig.4, p6-7, p10-p13|Cryogenian|Cryogenian|Amadeus Basin, including the Limbla Syncline. Re-Os date on an organic-rich shale from lowermost part of formation (Kendall et al., 2006).|Re-Os age 657.2+/-5.4 Ma||Includes Limbla Member, Ringwood Member.|Unconformably underlying Olympic Formation. Overlies Areyonga Formation.|Includes limestone and dolostone.|
524|Aralka Formation|72601|3|Fully described|p1-12, p14-15, p17-20, p24-25|Cryogenian|Cryogenian|Amadeus Basin, widespread. Deposited between the Sturt and Elatina glacial episodes. A Re-Os age of 657.2 +/- 5.4 Ma was reported by Kendall et al. (2006) from near the base of the formation. Estimated to have been deposited between ca 660 Ma and ca 635 Ma, which is comparable to constraints for the Cryogenian interglacial period. Stromatolite biostratigraphy was used for basin-scale correlation of the unit. The type section is 1019 m thick. Deposited in a marine environment including deep marine environments reflected in the lower portion of the unit. Dominated by siltstone, which occurs above and below two formal members. Potential hydrocarbon source rock with demonstrated capacity for gas and oil (see Marshall, 2005; Munson, 2014). Includes evidence for significant unroofing in the Amadeus Basin. Palynomorphs are scarce to absent despite suitable preservation potential.|657.2 +/- 5.4 Ma Re-Os||Ringwood Member, Limbla Member|Underlain by Areyonga Formation. Unconformably overlain by Olympic Formation and Pioneer Sandstone. Probably correlates with the lower part of the Umberatana Group.|Drillcore: interbedded black siltstone and mudstone with minor stromatolitic carbonate. Outcrop: carbonate strike bands separated by poorly exposed siltstone, and includes stromatolitic dolomite interbedded with distinctive intraclastic dolomite.|
524|Aralka Formation|73085|4|Described|piii, p1-3, p5, p15-16, p19-23, p26-27|Cryogenian|Cryogenian|Amadeus Basin. Contains diagnostic stromatolite taxa. 335.9 m thick in drillhole BR05DD01. Petrographic analyses notes siltstone is typically dolomitic (unlike underlying unit). Includes intraclast (or intraformational) breccia as seen in outcrop and drillcore. Also includes calcite veins and minor sulfides. Contact with the underlying Areyonga Formation is marked by the first occurrence of diamictite.|||Ringwood Member, Limba Member|Underlain by Areyonga Formation. Overlain by Pertatataka Formation and Pioneer Sandstone / Olympic Formation. Equivalent to Inindia beds.|Dark brown to dark grey, planar bedded siltstone; siltstone is carbonaceous and finely laminated with occasional grey, calcareous, laminated siltstone intervals; carbonate intervals are variably stromatolitic.|
524|Aralka Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Added reference area. Characterised as a poorly exposed, recessive siltstone dominated unit. Amadeus Basin. Part of Supersequence II. Undivided Aralka Formation siltstones referred to as lower, middle or upper Aralka Formation according to position relative to formal members; however, the definition card describes a Lower Aralka Formation and Upper Aralka Formation [not commonly referred to in the body of the text]. Previously included in the Pertatataka Formation (Wells et al., 1967). Also correlates to Rinkabeena Shale, Nabarula Formation, Wockerwirra and Tindelpina members (Tapley Hill Formation, Umbertana Subgroup, Heysen Supergroup), Balcanoona Formation. Partly equivalent to 'Undoolya Sequence'. p: 3, 5-6, 27, 53, 56-57, 61-63, 66, ~71-100, 114, 121-122, 126, 143, 158, 160-167, App 2.|658 +/- 5 Ma, 657.2 +/- 5.4 Ma Re-Os||Limbla Member, Ringwood Member|Underlain conformably by Areyonga Formation and unconformably by the Bitter Springs Group. Disconformably overlain by Olympic Formation. Correlates to lower Inindia beds and more [see comments].|Grey-green to red siltstone and shale with minor interbeds of fine-grained sandstone and carbonate rocks.|
524|Aralka Formation|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.|||Limbla Member, Ringwood Member|Unconformably underlain by Areyonga Formation. Unconformably overlain by Pioneer Sandstone and Olympic Formation.||
524|Aralka Formation|73180|4|Described|p47-48, p52-53|Neoproterozoic|Neoproterozoic|Amadeus Basin. Typifies the global post-glacial sequence of the Sturt glaciation. Local thickness variations in Areyonga-Aralka sequence from halotectonics within salt of the underlying Gillen Formation, created local highs scoured by the Elatina ice-sheet in the northeast side of the basin forming the Base Olympic/Pioneer Disconformity. Thinning of the Areyonga-Aralka package to the northeast due to low-angle truncation by the base of the overlying Pioneer Sandstone.  Accumulated within anoxic bottom waters beneath oxic surface waters.|||Ringwood Member, Limbla Member|Conformably overlies the Areyonga Formation, disconformably underlies the Olympic Formation and Pioneer Sandstone.|Dark grey to black organic-rich shales and siltstones with biomarkers of aerobic and anaerobic bacteria.|
524|Aralka Formation|73279|5|Briefly described|p3-5|Cryogenian|Cryogenian|Amadeus Basin. Non-glacial. Detrital zircons analysed for Hf isotopic composition [see article].|||Limbla Member||Includes sandstone.|
524|Aralka Formation|74367|5|Briefly described|p19|Cryogenian|Cryogenian|Amadeus Basin.|657.2+/-5.4 Ma Re-Os whole rock|||||
538|Arbitration Cove Sandstone Member|23722|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Parent: Warton Sandstone.   Geological Province: Kimberley Basin||||||07-NOV-08
538|Arbitration Cove Sandstone Member|30897|6|Mentioned|p13|||Stratigraphy||||||
538|Arbitration Cove Sandstone Member|36551|6|Mentioned|p33|||||||||
538|Arbitration Cove Sandstone Member|42814|6|Mentioned|p14|||of Warton Sandstone on Koolan Island||||||
571|Areyonga Formation|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Sandstone, arkose, tillitic siltstone, conglomerate, dolomite; phosphatic.  Geological Province: Amadeus Basin.||||||
571|Areyonga Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Calcareous sandstone, tillitic siltstone, conglomerate.||||||
571|Areyonga Formation|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
571|Areyonga Formation|22560|6|Mentioned|p4|||||||||
571|Areyonga Formation|22561|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22562|6|Mentioned|p39|||||||||
571|Areyonga Formation|22566|4|Described|p80|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
571|Areyonga Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22647|6|Mentioned|p 125||Neoproterozoic|Underlying Unit - Loves Creek Member of the Bitter Springs Formation p 114.||||||
571|Areyonga Formation|22648|6|Mentioned|p 135|||Overlying Unit - Pioneer Sandstone p 135.||||||
571|Areyonga Formation|22649|5|Briefly described|p 140|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22651|6|Mentioned|Fig 11 btw p182-183|Proterozoic|Proterozoic|||||||
571|Areyonga Formation|22761|6|Mentioned|p358|||||||||
571|Areyonga Formation|22763|5|Briefly described|p398|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22804|6|Mentioned|p429|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|22805|6|Mentioned|p464|||||||||
571|Areyonga Formation|22806|6|Mentioned|p478|Proterozoic|Proterozoic|||||||
571|Areyonga Formation|22807|6|Mentioned|p497||Neoproterozoic|||||||
571|Areyonga Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Amadeus Basin||||||
571|Areyonga Formation|22826|6|Mentioned|p568|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Correlate of Wilyerpa Formation and Holowilena Ironstone (Umberatana Group).||||||
571|Areyonga Formation|23282|6|Mentioned|p55|||of Amadeus Basin. Equivalent to Chambers Bluff Tillite.||||||
571|Areyonga Formation|23288|6|Mentioned|p142 Fig.18|||of Amadeus Basin.||||||
571|Areyonga Formation|23314|5|Briefly described|333 Fig.4|Cryogenian||||||||
571|Areyonga Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|24063|5|Briefly described|p219|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
571|Areyonga Formation|24064|5|Briefly described|p229 Fig.7|Adelaidean|Adelaidean|Geological Province: Amadeus Basin.||||||
571|Areyonga Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.  See also p215 Fig. 11.||||||
571|Areyonga Formation|24301|6|Mentioned|p16|||Geological Province: Amadeus Basin||||||
571|Areyonga Formation|29721|6|Mentioned|Table 44|||||||||
571|Areyonga Formation|29972|6|Mentioned|Table 1|||Lower Cambrian||||||
571|Areyonga Formation|30220|6|Mentioned|p245|||||||||
571|Areyonga Formation|30238|4|Described|p65|||Upper Proterozoic||||||
571|Areyonga Formation|30258|6|Mentioned|Fig.2|||Proterozoic age||||||
571|Areyonga Formation|30544|6|Mentioned|p48|||On map legend||||||
571|Areyonga Formation|31022|6|Mentioned|Fig. 4|||||||||
571|Areyonga Formation|31566|6|Mentioned|p230|||Proterozoic||||||
571|Areyonga Formation|31645|6|Mentioned|Table 2|||Correlation||||||
571|Areyonga Formation|31707|6|Mentioned|Table 1|||See also Fig. 2||||||
571|Areyonga Formation|32376|6|Mentioned|Table 3|||||||||
571|Areyonga Formation|32469|6|Mentioned|p531|||||||||
571|Areyonga Formation|32720|6|Mentioned|Table 1|||||||||
571|Areyonga Formation|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean||||||
571|Areyonga Formation|33025|6|Mentioned|p928|||||||||
571|Areyonga Formation|33102|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|33307|6|Mentioned|Fig.6|||||||||
571|Areyonga Formation|33729|6|Mentioned|p81|||U.Prot. Fauna.||||||
571|Areyonga Formation|33761|6|Mentioned|p146|||||||||
571|Areyonga Formation|33932|6|Mentioned|p11|||780my.||||||
571|Areyonga Formation|33934|6|Mentioned|p2395|||U. Prot.||||||
571|Areyonga Formation|34111|4|Described|Table 4|||Precambrian||||||
571|Areyonga Formation|34186|6|Mentioned|Fig.3|||Late Precambrian. See also Fig.4.||||||
571|Areyonga Formation|34201|6|Mentioned|p391|||Fauna||||||
571|Areyonga Formation|34202|6|Mentioned|p1057|||See also p1058.||||||23-APR-18
571|Areyonga Formation|34287|6|Mentioned|p39|||See also p41||||||23-APR-18
571|Areyonga Formation|34442|6|Mentioned|p7|||Proterozoic||||||
571|Areyonga Formation|34488|4|Described|Table 1|||Proterozoic. See also PP9,10,11 etc||||||
571|Areyonga Formation|34579|6|Mentioned|p15|||See also pp17,18.||||||23-APR-18
571|Areyonga Formation|34580|5|Briefly described|Table 1|||||||||
571|Areyonga Formation|35102|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|35485|6|Mentioned|p335|||||||||
571|Areyonga Formation|35805|5|Briefly described|p36|||See also Fig.3.||||||
571|Areyonga Formation|35863|6|Mentioned|Table 1|||||||||
571|Areyonga Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
571|Areyonga Formation|36898|6|Mentioned|p181|||See also Fig.4.||||||
571|Areyonga Formation|37238|6|Mentioned|p355|||||||||
571|Areyonga Formation|37371|6|Mentioned|p388|||||||||
571|Areyonga Formation|37462|4|Described|Table 4.IX|||||||||
571|Areyonga Formation|37928|3|Fully described|p515|||||||||
571|Areyonga Formation|37929|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|38157|6|Mentioned|Table VI|||||||||
571|Areyonga Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|39210|4|Described|p34|||Stromatolites||||||
571|Areyonga Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
571|Areyonga Formation|39565|6|Mentioned|p32|||||||||
571|Areyonga Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
571|Areyonga Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone with some erratics, feldspathic sandstone, conglomerate. dark grey cap dolomite. Geological Province: Amadeus Basin.||||||14-FEB-06
571|Areyonga Formation|40105|6|Mentioned|p311|||||||||
571|Areyonga Formation|40201|5|Briefly described|Table 1|||||||||
571|Areyonga Formation|40562|6|Mentioned|p684|||||||||
571|Areyonga Formation|40740|4|Described|p12|||||||||
571|Areyonga Formation|40852|6|Mentioned|p29|||||||||
571|Areyonga Formation|40856|5|Briefly described|p316|||||||||
571|Areyonga Formation|41005|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|41039|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|41115|6|Mentioned|p1390|||||||||
571|Areyonga Formation|41190|6|Mentioned|Fig.4|||||||||
571|Areyonga Formation|41203|5|Briefly described|p28|||Mention p5.||||||23-APR-18
571|Areyonga Formation|41224|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|41233|6|Mentioned|Fig.3|||||||||
571|Areyonga Formation|41405|6|Mentioned|p205|||||||||
571|Areyonga Formation|41618|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|41639|6|Mentioned|p17|||||||||
571|Areyonga Formation|41717|5|Briefly described|p355|||||||||
571|Areyonga Formation|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
571|Areyonga Formation|41816|6|Mentioned|p18|||||||||
571|Areyonga Formation|42059|5|Briefly described|p130|||See also Fig.2||||||
571|Areyonga Formation|42060|6|Mentioned|Fig.5 P140|||||||||
571|Areyonga Formation|42082|6|Mentioned|Fig.3 P323|||||||||
571|Areyonga Formation|42504|5|Briefly described|p69|||||||||
571|Areyonga Formation|42643|6|Mentioned|Fig.4 P19|||||||||
571|Areyonga Formation|42652|5|Briefly described|Fig. 13-1|||||||||
571|Areyonga Formation|42845|6|Mentioned|Fig.2 P497|||||||||
571|Areyonga Formation|42886|5|Briefly described|Fig.2 P219|||||||||
571|Areyonga Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Siltstone, diamictite, sandstone, dolostone.  Geological province: Amadeus Basin.||||||23-JAN-08
571|Areyonga Formation|43052|5|Briefly described|p198|||||||||
571|Areyonga Formation|43105|5|Briefly described|Fig.3,p8|||||||||
571|Areyonga Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||22-DEC-09
571|Areyonga Formation|43230|6|Mentioned|p9||Neoproterozoic|Reservoir target.||||||
571|Areyonga Formation|43503|6|Mentioned|11-50|||age from Ediacaran||||||
571|Areyonga Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|Age: approx 725 Ma||||||
571|Areyonga Formation|43648|6|Mentioned|Fig.27,p509|||||||||
571|Areyonga Formation|43649|5|Briefly described|p457|||||||||
571|Areyonga Formation|43817|6|Mentioned|Fig.1,p42|||||||||
571|Areyonga Formation|44261|14|Not recorded|p7-19|||Not recorded on white card.||||||
571|Areyonga Formation|44262|14|Not recorded|p5,7|||||||||
571|Areyonga Formation|44327|14|Not recorded|p.8,13|||Correlation with Mount Cornish Formation.||||||
571|Areyonga Formation|44335|4|Described|p.7||Proterozoic|Tb.1,p.8.||||||
571|Areyonga Formation|44336|14|Not recorded|map legend||Proterozoic|SG/53-3.||||||23-DEC-09
571|Areyonga Formation|44342|14|Not recorded|p.5|||SG/53-5, correlated with Inindia Beds.||||||
571|Areyonga Formation|44433|14|Not recorded|map legend||Proterozoic|||||||
571|Areyonga Formation|44484|14|Not recorded|p.9,10,13,Tb.1,Fig.4||Proterozoic|||||||
571|Areyonga Formation|44485|14|Not recorded|map legend||Proterozoic|||||||
571|Areyonga Formation|44497|4|Described|p.6, Table 1||Proterozoic|SF/53-13.||||||
571|Areyonga Formation|44498|14|Not recorded|map legend||Proterozoic|||||||22-DEC-09
571|Areyonga Formation|44499|14|Not recorded|opp.p.6, Tb.1||Proterozoic|||||||
571|Areyonga Formation|44505|14|Not recorded|p.7,11,Table 1,Fig 1||Proterozoic|||||||
571|Areyonga Formation|44506|14|Not recorded|map legend||Proterozoic|||||||
571|Areyonga Formation|45041|4|Described|p37|||Lateral equiv. Pertatataka Fm.||||||
571|Areyonga Formation|45052|6|Mentioned|p67|||Correlation with Field River Beds||||||
571|Areyonga Formation|45149|6|Mentioned|p21|||||||||
571|Areyonga Formation|45155|6|Mentioned|Fig.7|||Amadeus Basin||||||
571|Areyonga Formation|45170|6|Mentioned|Table 3|||||||||
571|Areyonga Formation|46829|6|Mentioned|Fig.2|||||||||
571|Areyonga Formation|46865|4|Described|p52|||||||||
571|Areyonga Formation|46903|6|Mentioned|Fig.5|||Correlation chart||||||
571|Areyonga Formation|46928|6|Mentioned|Table 1|||||||||
571|Areyonga Formation|48639|14|Not recorded|opp.p.1,map||Cretaceous|Cret.||||||
571|Areyonga Formation|48838|2|Defined|p.12, Tb.I|||||||||
571|Areyonga Formation|48842|14|Not recorded|p.12,16,Tb.I|||Equivalent to Carnegie & Boord Formations.||||||
571|Areyonga Formation|48844|14|Not recorded|p.20|||||||||
571|Areyonga Formation|48862|14|Not recorded|p.8|||Opp.9. (F52-15).||||||
571|Areyonga Formation|48863|2|Defined|p.11||Neoproterozoic|Tb.1, opp.p.7,8,12,16,17,19,20,40,41,42,pl.1,15,16. Upper Proterozoic. (G/53-1).||||||18-JUL-06
571|Areyonga Formation|48864|14|Not recorded|p.1,10,27||Neoproterozoic|Tb.1,opp.p.6, U.Prot.||||||
571|Areyonga Formation|48865|14|Not recorded|p.5,9,Fig.4,13|||Equiv.to part of Inindia Beds. (G52-4,F53-13).||||||
571|Areyonga Formation|48880|14|Not recorded|p.29,30,Pl.10-13||Neoproterozoic|(F53-13,14,15,G53-3). U.Prot.||||||
571|Areyonga Formation|48890|4|Described|p.21||Neoproterozoic|See also Tables, Figs, Plates. Equiv. Inindia Beds, Upper Proterozoic. Defn. on Tech.File F/53-13.||||||
571|Areyonga Formation|48963|6|Mentioned|p5|||||||||
571|Areyonga Formation|49796|5|Briefly described|Sect C BDF 28|||||||||
571|Areyonga Formation|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, arkose, tillitic sandstone, conglomerate, dolomite; phosphatic. Geological Province: Amadeus Basin.||||||
571|Areyonga Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone with some erratics, feldspathic sandstone, conglomerate, diamictite, rare dark cap dolomite.||||||
571|Areyonga Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
571|Areyonga Formation|61732|5|Briefly described|p4 Fig. 3|Sturtian|Sturtian|Overlain by the Aralka Formation. Geological Province: Amadeus Basin.||||||07-FEB-11
571|Areyonga Formation|62379|5|Briefly described|p7 Fig. 2, p30|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Coarse conglomerate, sandstone, siltstone and shale||||||
571|Areyonga Formation|62453|5|Briefly described|p12 Fig. 8|Cryogenian|Cryogenian|Geological Province: Amadeus Basin.||||||
571|Areyonga Formation|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and tillitic claystone, sandstone, dolomite. Underlies; Pertataka Formation. Overlies: Bitter Springs Formation.||||||14-AUG-06
571|Areyonga Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and tillitic claystone, sandstone, dolomite.||||||
571|Areyonga Formation|62903|6|Mentioned|p729, p730 Fig.1|||Amadeus Basin. Correlated with Sturtian glacial deposits (Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites and Wilyerpa-Lyndhurst Formations). Age is for base of overlying Aralka Formation. Presented in figure as Areyonga.||||is overlain conformably by Aralka Formation|glacial; diamictites|
571|Areyonga Formation|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|Amadeus Basin.||||Is overlain by Aralka Formation.||
571|Areyonga Formation|63562|5|Briefly described|p338 fig 3, p342, p343, p352 fig 10|Cryogenian|Cryogenian|Of Amadeus Basin. Deposits of ice flow from north and progradation of siliciclastic sediments from south.||||Correlated with Mount Cornish Formation. Is overlain by Aralka Formation.|Includes tillites from Sturtian glaciation.|
571|Areyonga Formation|64068|6|Mentioned|p45, 223|||Amadeus Basin. Correlated with Yardida Tillite, southern Georgina Basin.||||||
571|Areyonga Formation|64103|6|Mentioned|p404|||Geological Province: Amadeus Basin.||||||07-FEB-11
571|Areyonga Formation|64625|5|Briefly described|p245 fig 2, p257|||Amadeus Basin. Correlated with the Sturtian glacial event in the Adelaide Rift Complex.||||Unconformably overlies Bitter Springs Formation or Johnny's Creek beds. Is overlain by Aralka Formation.|Sandstone, dolomite and diamictite.|
571|Areyonga Formation|64677|6|Mentioned|v, p1, p15-20, p49-50|Neoproterozoic|Neoproterozoic|Eastern Amadeus Basin. A sample of this (presumed) unit included a tuff dated at 224.4 +/- 2.8 Ma (Triassic). The sampled rock "may belong to a younger succession".||||||
571|Areyonga Formation|64778|6|Mentioned|p13, 18|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
571|Areyonga Formation|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|The rank is not shown in Fig.2.||||||
571|Areyonga Formation|64796|6|Mentioned|p186 Fig.4, p200 Fig.10|||||||||
571|Areyonga Formation|64797|5|Briefly described|p153 Fig.2, p156, p157 Tb.2, p164 Fig.11|||See also p168 Tb.11. S-isotope data.||||contacts Aralka Formation.||
571|Areyonga Formation|64809|4|Described|p2, p3 Fig.2, p6 Fig.4, p7|Proterozoic|Proterozoic|Northern Amadeus Basin. Paralic deposition. Sourced partly from Arunta Metamorphic Complex.||||Unconformably overlies the Bitter Springs Formation.|Consists of diamictite, conglomerate, sandstone and dolostone.|
571|Areyonga Formation|64970|6|Mentioned|p719 Fig. 2, p726|Sturtian|Sturtian|Age: ~760Ma. Geological Province: Amadeus Basin.||||||27-MAY-09
571|Areyonga Formation|65233|4|Described|p3 Fig. 2, p6|Neoproterozoic|Neoproterozoic|Overlain by Aralka Fm; unconformable below Pertatataka Formation also. Geol.prov: Amadeus Basin. Together with Aralka Fm, this glaciogenic succession shows marked lith. variation (details included).||||||07-FEB-11
571|Areyonga Formation|65272|5|Briefly described|p318, p320, p323, p326-329||Cryogenian|Related to the Sturtian glaciation. 40Ar/39Ar data. Results imply the presence of c.5 to 6 km of overlying sediment before Paleozoic unroofing.||||Unconformably overlies Bitter Springs Formation.|Diamictite conglomerate, calcareous and lithic sandstone.|
571|Areyonga Formation|65365|5|Briefly described|p7, 9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Amadeus Basin. Diamictite, postulated Sturtian glaciation age.||||Unconformably overlies Finke beds.||19-MAR-12
571|Areyonga Formation|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Amadeus Basin. Diamictite, postulated Sturtian glaciation age||||||
571|Areyonga Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 2.||||||
571|Areyonga Formation|65489|5|Briefly described|p125|Proterozoic|Proterozoic|Amadeus Basin. Hosts Doraminna 1 gas discovery.||||Unconformably overlies Bitter Springs Formation.||
571|Areyonga Formation|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|Amadeus Basin. 400-500m thick. Diamictite is associated with the Sturtian glaciation.||||Overlies Loves Creek Member (Bitter Springs Formation). Is overlain conformably by Aralka Formation.|Dominated by glacial diamictite (tillite), with thin interbeds of sandstone, conglomerate, shale and siltstone, and dolostone.|
571|Areyonga Formation|67326|5|Briefly described|p2, p8-9, p11, Appx.2|Neoproterozoic|Neoproterozoic|Amadeus Basin. A 48m thick glacigene succession. Correlated with c.730 Ma Sturtian glacials in the Adelaide Fold Belt. Many clasts were sourced from underlying Bitter Springs Formation. Core section photograph. Composite log.||||Unconformably overlies Bitter Springs Formation. Is overlain by Aralka Formation.|Massive diamictite.|
571|Areyonga Formation|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Amadeus Basin.||||Is overlain by Aralka Formation.||
571|Areyonga Formation|67565|6|Mentioned|p5 Fig.3.|||Amadeus Basin.||||||
571|Areyonga Formation|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Amadeus Basin.||||Is overlain by Aralka Formation.||
571|Areyonga Formation|67856|6|Mentioned|p338 fig 4-30, p337, 339, 344, 345, 348|Neoproterozoic|Neoproterozoic|||||Unconformably overlies Bitter Springs Formation.||
571|Areyonga Formation|68244|6|Mentioned|p671|Neoproterozoic||Amadeus Basin. Minimum age of 657.2+\-5.4 Ma by Kendall et al., 2006.||||||
571|Areyonga Formation|68270|4|Described|p679,683-684,687-688|Cryogenian|Cryogenian|Amadeus Basin. Type section is in Ellery Creek, 1.5km south of contact with basement; lat.23'47'S, long. 133'04'E. Less than 250m thick. Subglacial, ice-margin, shallow-marine ice proximal deposit. Clast types are variable and derived from both intrabasinal (carbonate, chert, quartzite and conglomerate) and extrabasinal (granite, gneiss, porphyry, volcanic rocks and schist) sources (Lindsay 1989). Includes a 'lower marker cap dolomite' related to Sturt glaciation. Correlative to Sturt Tillite.||||Overlain conformably to disconformably by Aralka Formation. Underlain unconformably by Johnnys Creek beds or Bitter Springs Formation (karstified surface).|Diamictite (<1 m to >40 m) of variable composition and texture with thinner interbeds of sandstone, conglomerate and carbonate.|03-JUL-19
571|Areyonga Formation|68276|6|Mentioned|p68|Neoproterozoic|Neoproterozoic|"The ""Formation"" is omitted."||||||
571|Areyonga Formation|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
571|Areyonga Formation|68316|6|Mentioned|p778 Fig.1|||||||||
571|Areyonga Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
571|Areyonga Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
571|Areyonga Formation|68733|6|Mentioned|p189 Fig.8|Cryogenian|Cryogenian|Amadeus Basin.||||Equivalent to Lower Inindia Beds.||04-DEC-17
571|Areyonga Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||||
571|Areyonga Formation|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|NE Amadeus Basin, Centralian A Superbasin. Supersequence 2.||||Is overlain by Aralka Formation.|Includes tillite.|12-JUL-16
571|Areyonga Formation|69438|3|Fully described|p23:2-7, 10, 15-18, 21, 27-29, 42-43, 47|Cryogenian|Cryogenian|See also 23:53, 59-60. Pritchard and Quinlan (1962) first defined this unit with two Members from the section at Ellery Creek type area. Redefined by Priess et al. (1978) who reassigned the upper Member to the overlying Pioneer Sandstone. Amadeus Basin. c.250m thick. Is correlated with Inindia beds and other Sturtian (Neoproterozoic) glacial successions in the Adelaide Fold Belt, Georgina and Ngalia Basins, and the Kimberley region. Hosts the Ringwood copper occurrence. One of the most likely oil- and/or gas-prone units in the Basin; has promising Neoproterozoic hydrocarbon reservoirs, and gas flows in Ooraminna-1 and -2. Sealed by thick Aralka Formation shales.||||Overlies Finke beds, Bitter Springs Formation disconformably. Is overlain disconformably by Pioneer Sandstone and Chandler Formation, unconformably by Tempe Formation, conformably by Aralka Formation.|Mainly diamictite (tillite) with thin interbeds of sandstone, conglomerate, shale and siltstone, and a "cap" dolostone. Diamictite clasts have diverse compositions, with more or less uniform matrix, massive, poorly sorted and generally grey-green.|12-JUL-16
571|Areyonga Formation|69439|6|Mentioned|p24:7|||Amadeus Basin.||||Correlated with Naburula Formation.||12-JUL-16
571|Areyonga Formation|69443|6|Mentioned|p28:8|||Amadeus Basin.||||Equivalent to the Aroota Group.||12-JUL-16
571|Areyonga Formation|69606|5|Briefly described|p1, p3, p4 fig 2, p5, p6 fig 3, p7 fig 4|Cryogenian|Cryogenian|Of Supersequence 2. c. 150m thick. Potential source and seal rock. Amadeus Basin. Glacigene unit, correlated with the Sturt Glaciation of the Adelaide Rift Complex. See also p8, p9 fig 5, p10, p11 fig 6, p12.||||Overlain by the Aralka Formation|Glacial diamictite with interbeds of sandstone, conglomerate and carbonate.|
571|Areyonga Formation|69673|5|Briefly described|p63,p71, p81, p88, p89, p91, p98|||Up to 250m thick. Also correlated with Inindia beds and disconformably overlies Bitter Springs Formation.||||Overlain by Aralka Formation. Unconformably overlies Finke beds, Johnnys Creek beds. Disconformably overlain by Chandler Formation, Pioneer Sandstone|Tillite with thin interbeds of sandstone, conglomerate, shale, siltstone and dolostone.|
571|Areyonga Formation|69937|4|Described|v-vi, p3 Tb.1, p8, p11-13, p41-42|Neoproterozoic|Neoproterozoic|Amadeus Basin. Fluvial to glacigene deposits; correlated with the 700-690 Ma Sturtian glacial successions, and considerably younger than the youngest zircon. Likely zircon provenance discussed.|876 +/- 14 Ma (maximum depositional age).|||Disconformably overlies Bitter Springs Formation. Is overlain conformably by Aralka Formation and disconformably by Olympic Formation.|Mainly diamictite, with interbeds of sandstone, conglomerate, shale, siltstone and dolostone.|
571|Areyonga Formation|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 2 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain by Aralka Formation. Underlain by Johnny's Creek Member/Bitter Springs Formation.||
571|Areyonga Formation|70416|5|Briefly described|p63, p65|Cryogenian|Cryogenian|Amadeus Basin. The base of this unit has a Basin-wide unconformity marking the start of Cryogenina Supersequence 2. Glacigenic. Earlier definitions included rocks subsequently assigned to Aralka Formation.||||Unconformably overlies Wallara Formation. Is overlain conformably by Aralka Formation.||
571|Areyonga Formation|70634|6|Mentioned|194794.1.pdf|||||||||
571|Areyonga Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Aralka Formation. Underlain by Wallara Formation.||
571|Areyonga Formation|71001|5|Briefly described|p18 Fig.2, p19-20, 23, 27-28|Cryogenian|Cryogenian|Amadeus Basin. Glacial deposits. Cap carbonate is dominated by manganiferous dolomite. Carbon isotope correlation graph.|~720-668 Ma.|||Unconformably overlies Johnnys Creek Formation (Bitter Springs Group). Is overlain by Aralka Formation.|Diamictite; cap carbonate.|
571|Areyonga Formation|71080|5|Briefly described|p27, p29 fig 20, p30|Cryogenian|Cryogenian|Amadeus Basin. Base of  supersequence 2. Includes glacial diamictites.|||||Dominantly diamictite in WA. Includes sandstone, conglomerate in NT.|
571|Areyonga Formation|71088|6|Mentioned|p8, p15|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Correlated with the Carnegie Formation.||
571|Areyonga Formation|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
571|Areyonga Formation|71344|4|Described|p1094, 1093, 1096-1103|Cryogenian||Amadeus Basin. Glaciogenic succession. Capped by a very homogeneous grey dolostone, which forms a prominent marker horizon and is otherwise described as cap carbonate.||Of Inindia Package.||Unconformably overlies Bitter Springs Package [Wallara Formation?]|Diamictite interbedded with sandstone, conglomerate, shale, and minor dolostone.|
571|Areyonga Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|876+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Immature  medium- to coarse-grained quartz sandstone, fine-grained tuffaceous siltstone.|
571|Areyonga Formation|71801|6|Mentioned|p230-p231|Cryogenian|Cryogenian|Amadeus Basin.||||Overlain by the Aralka Formation.||
571|Areyonga Formation|71810|5|Briefly described|Map legend.|Cryogenian|Cryogenian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Diamictite and conglomerate; rare glacially faceted and striated clasts, very poorly exposed.|
571|Areyonga Formation|71841|5|Briefly described|iii,p1-7,9-13,15|Cryogenian|Cryogenian|Of Amadeus Basin. Original stratigraphy based on McKinnon-Matthews (2009): CPD001: 0-116.4m (EOH). CPD2: 65.9-176.65m. CPD003: 0-12m. Revised stratigraphy in drill core: CPD001: 101-116.4m (EOH). CPD002: 47-118.1m. CPD003: 0-12m, 152.8-172m (repetitive stratigraphy interpreted as due to CPD003 intersecting a series of faults and an overturned anticline, resulting stratigraphic repetition and reverse younging of the succession).  See p3-4 (CPD001), p6 (CPD002), p9-11 (CPD003) for lithological descriptions based on revised drill core intervals. ||||Overlain by Aralka Formation. Underlain by Bitter Springs Group or Wallara Formation. Grades into Inindia beds.||
571|Areyonga Formation|71842|4|Described|iii,p1-6,9|Cryogenian|Cryogenian|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT). Correlated with deposits of late Neoproterozoic Sturtian glaciation. Exposed in low to prominent arcuate strike ridges surrounding Mount Conner.|||Includes Conner Member.|Overlain by Aralka Formation. Underlain by Finke Beds or Wallara Formation or Bitter Springs Group. Correlable with Inindia beds.|Sandstone, mudstone, diamictite (mudstone matrix and angular clasts) and conglomerate facies.|
571|Areyonga Formation|71898|5|Briefly described|p6|||Amadeus Basin.||||Unconformably (possibly) overlain by the Quandong Conglomerate.|Massive-bedded sandstone.|
571|Areyonga Formation|72369|5|Briefly described|p7,9|||Of Amadeus Basin.||||Overlain unconformably by Aralka Formation.||
571|Areyonga Formation|72374|4|Described|iii,p3-4,6-11|||Of Amadeus Basin. Depositional environment: fluvial, glacigene. Deposited during Cryogenian Sturtian glaciation (c. 720-660 Ma; Rooney et al 2015). Correlated with glacial successions in the Adelaide Rift Complex (SA), the Ngalia and Georgina basins (NT) and Kimberley Region (WA) (see Edgoose 2013). Previous U-Pb SHRIMP and Hf isotope LA-ICP-MS geochronological studies (Kositcin et al 2015, Normington et al 2019) suggested a dominant sediment source from the Aileron and Warumpi provinces, including a subordinate 880 Ma zircon contribution from the underlying Bitter Springs Group. Sample HB16ND421 (coarse- to very coarse grained sandstone) yielded an interpreted maximum depositional age of 964+\-7 Ma. Includes late Paleo- to Mesoproterozoic zircons (c. 1800 to 1500 Ma, peaks at c. 1630 and c. 1590 Ma) derived from the Aileron and Warumpi provinces to the north, and Musgrave Province to the south. Subordinate Mesoproterozoic to Neoproterozoic (c. 1300 to c. 1100 Ma, c. 1050-830 Ma) were likely sourced from the Musgrave Province. Sample HB16ND422 (very coarse- to coarse grained quartz arenite) yielded an interpreted maximum depositional age of 907+\-6 Ma, including significant zircon population derived from Musgrave Province, or elsewhere in east Gondwana.|964+\-7 Ma|||Underlain by Bitter Springs Group. Correlatable to Inindia beds.|Predominantly diamictite, includes interbeds of sandstone, conglomerate, shale, siltstone, and carbonate.|11-OCT-19
571|Areyonga Formation|72375|4|Described|p1-2,13,15,17-19|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Fluvial to glacigene (Prichard and Quinlan 1962). Forms topographic highs and ridges, where outctop is locally stepply dipping and variably micaceous and silicified on ILLOGWA CREEK 1:100 000 mapsheet. SHRIMP U-Pb zircon analysis by Kositcon et al., 2015 yielded an interpreted (weighted mean 238U/206Pb) max depositional age of 876+\-14 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS IC13CJE018 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p17-18 for Hf isotopic results and interpretations). The lowermost part of this unit above the disconformity with the Johnnys Creek Formation was subsequently renamed and formalised as the Wallara Formation. Sample location and description is discussed.||||Overlain conformably by Aralka Formation. Underlain disconformably by Wallara Formation or Bitter Springs Group.|Diamictite, includes significant intervals of sandstone, conglomerate, shale, siltstone, and dolostone.|04-DEC-19
571|Areyonga Formation|72489|5|Briefly described|p3, p4 Fig.3, p10, p11|Cryogenian|Cryogenian|Amadeus Basin, including the Limbla Syncline. Re-Os date on an organic-rich shale from lowermost part of formation (Kendall et al., 2006). Local age: Sturtian.||||Overlies Bitter Springs Group. Underlies Aralka Formation.|Glacial deposits.|
571|Areyonga Formation|72516|6|Mentioned|p86|Cryogenian|Cryogenian|Amadeus Basin.||||Equivalent to the Mount Cornish Formation.||02-JUN-21
571|Areyonga Formation|72601|5|Briefly described|p3-5, p7-9, p11-12, p14, p17, p25|Cryogenian|Cryogenian|Amadeus Basin. Deposition was coeval with the Sturt glaciation. Includes potential hydrocarbon source rocks.|||Conner Member|Unconformably underlain by Wallara Formation. Overlain by Aralka Formation.|Includes a cap carbonate and diamictite.|
571|Areyonga Formation|73085|4|Described|p: iii, 1, 3, 5, 15-16, 19-20, ~22-27|Cryogenian|Cryogenian|Amadeus Basin. Records Sturtian glacial event[?]. Sharp contact with the overlying Aralka Formation and underlying Wallara Formation.||||Underlain by Wallara Formation. Overlain by Aralka Formation. Equivalent to Inindia beds.|Red-brown matrix-dominated siltstone diamictite with rare grey siltstone diamictite increasing in abundance towards the base of the unit.|
571|Areyonga Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Added reference area at Ellery Creek; necessary due to the variable lithology types. Characterized by poorly exposed diamictite or sandstone. Amadeus Basin. Part of Supersequence II. Glacigenic; associated with the Sturtian glaciation. Disconformably cuts into different levels of the underlying strata due to glacial scouring. Age is constrained by the timing of this glacial period. Diamictite includes intrabasinal clasts (i.e., Heavitree Formation, Bitter Springs Group and basement rocks). Two members were previously described but the younger of the two was later redefined as the Pioneer Sandstone. No known fossils. Maximum depositional age of 876 +/- 14 Ma is considerably older than the interpreted true depositional age. Can be difficult to distinguish from the Olympic Formation based on lithology alone. Reference area consists of 3 broad lithological groups [see definition card for detailed description]. Correlates to Nabarula Formation, Mount Cornish Formation, Yardida Tillite, Sturt Tillite and in part to Inindia beds. Partly equivalent to 'Undoolya Sequence'. Preveiously called No 2 quartzite [also written as No. 2 quartzite] [see p62, p157]. p: 3, 5-6, ~15-18, 39-40, 53, 56-72, 79, 91, 98-101, 112-114, 143, 151, 156-160, 166-167, App 2.|ca 720-660 Ma|||Unconformably underlain by Wallara Formation and Bitter Springs Group (all constituents). Overlain transitionally by Aralka Formation including the Ringwood Member. [See comments].|Diamictite (including erratic fields), sandstone, dolomitic arkose, conglomerate and dolomite with dolomitic silty shale at the top.|
571|Areyonga Formation|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Unconformably underlain by Wallara Formation. Unconformably overlain by Aralka Formation.||
571|Areyonga Formation|73180|4|Described|p47-49, 51 Fig.6, p53-54|Neoproterozoic|Neoproterozoic|Amadeus Basin. First recognised by Mawson (1957). Formally defined by Prichard and Quinlan (1960) with the type section within Ellery Creek, northern margin of the basin. Preiss et al (1978) and Lindsay (1989) described the unit and its lithology. Sturt glacial/post-glacial sequences. Locally the lower diamictites fill gullies scoured through the basal quartzites into underlying rocks.  Seismic imaging of a large mound of sediment interpreted as a diamictite grounding zone wedge deposited directly on the Base Areyonga Disconformity within the southeast side of the basin, further west the formation is dominated by shallow marine shales and siltstones with rare dropstones and pods of diamictite. Sediment was supplied subgacially from the southeast through a tunnel valley. Thinning of the Areyonga-Aralka package to the northeast due to low-angle truncation by the base of the overlying Pioneer Sandstone.||||Disconformably overlies the Wallara Formation and Bitter Springs Group, conformably underlies the Aralka Formation.  Correlated to the Sturt Tillite.|Glaciogenic tillitic sandstones, greywackes. Contains basal fluvial quartzites, overlying diamictites hosting cross-bedded sandstones and conglomerates, and capped by diamictites grading upwards into siltstone with stromatolitic dolostone interbeds.|
578|Argyle Lamproite|41158|6|Mentioned|Table 22|||See also Table 24||||||
578|Argyle Lamproite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen.|||||Volcaniclastic olivine lamproite intruded by olivine-phlogopite lamproite dykes.|30-JUL-15
578|Argyle Lamproite|69597|6|Mentioned|p3|||||||||
578|Argyle Lamproite|69634|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1177-1177 Ma (Isotopic)||||Volcaniclastic olivine lamproite intruded by olivine-phlogopite lamproite dykes|
578|Argyle Lamproite|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|1177 Ma||||Volcaniclastic olivine lamproite intruded by olivine--phlogopite lamproite dykes|
578|Argyle Lamproite|70812|5|Briefly described|p12|||Mineralisation is described.||||||
578|Argyle Lamproite|71267|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv.|1177+\-47 Ma (isotopic)||||Volcaniclastic olivine lamproite intruded by olivine-phlogopite lamproite dykes|
578|Argyle Lamproite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin.|1177+/-47 Ma.||||Volcaniclastic olivine lamproite intruded by olivine--phlogopite lamproite dyke.|
613|Armadale Shale|30939|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
613|Armadale Shale|33044|6|Mentioned|Map 3|||Part of Cardup Gp.||||||
613|Armadale Shale|35058|6|Mentioned|p64|||||||||
613|Armadale Shale|36293|2|Defined|p73|Neoproterozoic|Neoproterozoic|Type section 483 m thick in Cardup Quarry is the thickest measured section of the unit, but total thickness may be considerably more.||Of Cardup Group.||Conformably overlies Neerigan Formation. Overlain unconformably by Quaternary alluvial deposits.|Black and white shales with minor sandstone and orthoquartzite.|19-DEC-13
613|Armadale Shale|36872|3|Fully described|p78|||||||||
613|Armadale Shale|37460|6|Mentioned|p178|||||||||
613|Armadale Shale|67135|6|Mentioned|p59 Fig.80.|||Shown as a unit suitable for clay mining.||||||
636|Arrowhead Shale|41622|5|Briefly described|Fig.4|||||||||
636|Arrowhead Shale|42352|5|Briefly described|p31|||||||||
638|Arrowsmith Sandstone|36293|2|Defined|p53|Proterozoic|Proterozoic|||||||
638|Arrowsmith Sandstone|36872|3|Fully described|p72|||||||||
638|Arrowsmith Sandstone|37460|6|Mentioned|p178|||||||||
638|Arrowsmith Sandstone|40307|6|Mentioned|Fig.2|||||||||
638|Arrowsmith Sandstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
638|Arrowsmith Sandstone|40347|6|Mentioned|p15|||||||||
638|Arrowsmith Sandstone|41271|6|Mentioned|p228|||||||||
693|Ascot Formation|12759|5|Briefly described|p43-7; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Quaternary||Defined as Ascot Beds (Playford et al.,1976); redefined as a Formation by Cockbain and Hocking (1989); the informal Jandakot Beds were incorporated into the Ascot Formation by Kendrick et al. (1991).  Max thickness is 20 and 30 m in the S and N of Perth.||||Locally overlies Leederville, Osborne Formations or Molecap, Poison Hill Greensands, unconformably.|Limestone, sand, shells and clay.|12-MAY-14
693|Ascot Formation|23768|5|Briefly described|p27, p145|Pliocene|Pliocene|Geological Province: Perth Basin.||||||11-SEP-09
693|Ascot Formation|24094|4|Described|p274, p278|Early Pleistocene|Late Pliocene|Overlies Osborne Formation (unconformable). Geological Province: Perth Basin||||||16-MAR-05
693|Ascot Formation|24464|5|Briefly described|p333|||Overlain by Bassendean Sand.||||||
693|Ascot Formation|41751|6|Mentioned|p8|||||||||
693|Ascot Formation|42473|6|Mentioned|p8|||||||||
693|Ascot Formation|42569|5|Briefly described|p81|||||||||
693|Ascot Formation|43062|4|Described|p23,Table 2,p18|||||||||
693|Ascot Formation|43197|5|Briefly described|Map Legend||Tertiary|||||||
693|Ascot Formation|43231|6|Mentioned|p10|Pleistocene|Pliocene|||||||
693|Ascot Formation|43347|4|Described|9|Pleistocene|Pliocene|||||||
693|Ascot Formation|44144|4|Described|p502 Tb.4-21, p520|Pliocene|Pliocene|No type section. Up to 2m thick shallow marine deposits.||||Overlain by Guildford Formation disconformably. Correlates with Yoganup Formation.|Grey medium- to coarse-grained sandy calcarenite.|
693|Ascot Formation|63745|4|Described|p61, p63|Early Pleistocene|Late Pliocene|Unconformably overlain by Guildford Formation. Marine deposits comprising shelly calcarenites, silty clay and glauconitic clay. Contains abundant molluscan fauna.||||||07-FEB-11
693|Ascot Formation|68811|5|Briefly described|p90|Quaternary|Neogene|One of a group of 'superficial sediments' described as being up to 90m thick.|||||Group description: Sand, limestone, silt and clay.|15-APR-20
693|Ascot Formation|70097|5|Briefly described|p20 Fig.4|Pliocene|Pliocene|Northern Perth Basin. Dandaragan Trough.||||Is overlain by Bassendean Sandstone.|Limestone.|30-SEP-16
693|Ascot Formation|70128|5|Briefly described|p449|Holocene|Neogene|Perth Basin.||||Unconformably overlies Kings Park Formation.||
698|Ashburton Formation|22484|4|Described|p80 Fig.9|||||||||
698|Ashburton Formation|22512|5|Briefly described|P283|||12000m maximum thickness.||||||18-JAN-07
698|Ashburton Formation|22682|5|Briefly described|Fig5,p10||Archean|Ashburton Province||||||03-MAR-10
698|Ashburton Formation|22905|5|Briefly described|p53|Paleoproterozoic|Paleoproterozoic|Overlain by Edmund Group.||||||07-NOV-08
698|Ashburton Formation|23047|6|Mentioned|36 fig 2|||In the Hamersley Province.||||||10-FEB-09
698|Ashburton Formation|23280|6|Mentioned|Table1p1085|||||||||
698|Ashburton Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
698|Ashburton Formation|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit Capricorn Formation. Underlying unit June Hill Volcanics.||||||
698|Ashburton Formation|23612|5|Briefly described|p839|||Geological Province: Hamersley Basin.||||||
698|Ashburton Formation|23774|4|Described|p731-733|||Thorne and Seymour (1991). Also see p743. Overlain by Bangemall Supergroup - unconformable. Underlain by June Hill Volcanics - unconformable.||||||18-JAN-07
698|Ashburton Formation|23890|5|Briefly described|p5 Fig.2|||Geological Province: Ashburton Basin.||||||
698|Ashburton Formation|24183|6|Mentioned|p7|||Overlain by the Yilgatherra Formation.||||||
698|Ashburton Formation|24544|4|Described|p47|Paleoproterozoic|Paleoproterozoic|Of Upper Wyloo Group. Conformably overlies Duck Creek Dolomite and June Hill Volcanics. Mudstone and sandstone, minor conglomerate, BIF, chert, dolomite, volcanics. Channel to deep marine. Thickness: 5-12km. Geological Province: Ashburton Province.||||||07-NOV-08
698|Ashburton Formation|24602|4|Described|p853, p860, p854 Fig. 1|||Also referred to as Ashburton turbidites. Comprises 2 siliciclastic successions, previously mapped as a single unit; the older Ashburton Fm. is in type area south of Paraburdoo Hinge Zone and younger 'Ashburton' succession is north of Wyloo Dome.||||||12-JUN-13
698|Ashburton Formation|24607|3|Fully described|p967|Paleoproterozoic|Paleoproterozoic|Max. thickness: difficult to assess, estimated 5-12 km. Age from tuff in uppermost Ashburton Fm, Capricorn Range: 1806 +/- 9 Ma. Geological Province: Ashburton Basin.||Of the Wyloo Group||Conformably overlies the Duck Creek Dolomite and overlain by[?]/interfingers with June HIll Volcanics. Unconformably overlain by Capricorn Group.||23-DEC-15
698|Ashburton Formation|29716|4|Described|Table 1|||||||||
698|Ashburton Formation|29845|6|Mentioned|p162|||||||||
698|Ashburton Formation|29848|6|Mentioned|p413|||||||||
698|Ashburton Formation|33544|6|Mentioned|p286|||||||||
698|Ashburton Formation|34066|4|Described|p8|||See also P9. L.Prot. Of the Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|34124|4|Described|Table 1|||Lower Proterozoic. Of the Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|34135|4|Described|Table 2|||Lower Proterozoic. Of the Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|35218|6|Mentioned|Fig.1|||||||||
698|Ashburton Formation|35260|5|Briefly described|p18|||||||||
698|Ashburton Formation|35726|6|Mentioned|p36|||||||||
698|Ashburton Formation|35976|6|Mentioned|Fig.38|||See also Table 16.||||||
698|Ashburton Formation|36551|6|Mentioned|p22|||See also Table 23.||||||
698|Ashburton Formation|36880|6|Mentioned|p108|||||||||
698|Ashburton Formation|36882|4|Described|p136|||||||||
698|Ashburton Formation|36891|5|Briefly described|p442|||||||||
698|Ashburton Formation|36902|6|Mentioned|p15|||||||||
698|Ashburton Formation|37327|5|Briefly described|p397|||||||||
698|Ashburton Formation|37460|3|Fully described|p121|||||||||
698|Ashburton Formation|38321|6|Mentioned|Table 1|||||||||
698|Ashburton Formation|38482|6|Mentioned|p15|||See also Table 4.||||||
698|Ashburton Formation|38790|6|Mentioned|p161|||||||||
698|Ashburton Formation|39210|5|Briefly described|Table 1|||||||||
698|Ashburton Formation|40103|6|Mentioned|Fig.1|||||||||
698|Ashburton Formation|40369|6|Mentioned|p17|||||||||
698|Ashburton Formation|40554|5|Briefly described|p30|||||||||
698|Ashburton Formation|40905|6|Mentioned|Fig.1|||||||||
698|Ashburton Formation|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
698|Ashburton Formation|40937|6|Mentioned|p3|||||||||
698|Ashburton Formation|41125|6|Mentioned|p28|||||||||
698|Ashburton Formation|41243|6|Mentioned|p258|||||||||
698|Ashburton Formation|41845|6|Mentioned|Fig. 1|||||||||
698|Ashburton Formation|41846|6|Mentioned|p94|||||||||
698|Ashburton Formation|41955|6|Mentioned|Fig.1 P4|||||||||
698|Ashburton Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
698|Ashburton Formation|42148|6|Mentioned|Table 1 P687|||||||||
698|Ashburton Formation|42260|3|Fully described|p59|||||||||
698|Ashburton Formation|42277|5|Briefly described|p55|||See also Fig. 1||||||
698|Ashburton Formation|42435|4|Described|p46|||||||||
698|Ashburton Formation|42471|4|Described|p12|||||||||
698|Ashburton Formation|42472|5|Briefly described|Map legend|||||||||23-DEC-09
698|Ashburton Formation|42686|5|Briefly described|map legend|Proterozoic||||||||
698|Ashburton Formation|42704|5|Briefly described|Plate 2E|Proterozoic||Of the Wyloo Group. Sandstone, mudstone, dolomite. Intruded by dolerite sills.||||||07-AUG-08
698|Ashburton Formation|42730|6|Mentioned|p13|||In the upper Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|42744|4|Described|p7|||||||||
698|Ashburton Formation|43037|5|Briefly described|Fig.2,p24|||of Wyloo Group||||||
698|Ashburton Formation|43119|5|Briefly described|p15|||of Wyloo Group||||||
698|Ashburton Formation|43262|5|Briefly described|Map Legend||Proterozoic|f the Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|43290|4|Described|p10||Proterozoic|Of the Wyloo Group.||||||18-JAN-07
698|Ashburton Formation|43595|5|Briefly described|Table 3-8,p344||Paleoproterozoic|||||||07-NOV-08
698|Ashburton Formation|44142|6|Mentioned|p311 fig 4-15|||||Wyloo Group.||Is overlain unconformably by Irregully Formation.||
698|Ashburton Formation|44319|14|Not recorded|map legend||Paleoproterozoic|Wyloo Group. L.Proterozoic.||||||07-NOV-08
698|Ashburton Formation|44477|4|Described|p.12, Table 1||Proterozoic|SF/50-6.||||||
698|Ashburton Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
698|Ashburton Formation|44481|5|Briefly described|map legend||Proterozoic|||||||
698|Ashburton Formation|44692|2|Defined|p.17,19, Tb.1, map|||Iron Ore. (F50-11).||||||
698|Ashburton Formation|44729|5|Briefly described|map legend|Proterozoic||Of Wyloo Group||||||
698|Ashburton Formation|50010|6|Mentioned|p55 Fig. 1|Mesoproterozoic|Mesoproterozoic|||||||
698|Ashburton Formation|50216|6|Mentioned|p208|||||||||30-MAR-05
698|Ashburton Formation|50225|5|Briefly described|p390|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Yilgatherra Formation (Edmund Group).||||||07-FEB-11
698|Ashburton Formation|50226|5|Briefly described|p415, p416|Paleoproterozoic|Paleoproterozoic|Of the upper part of the Wyloo Group.  Predominantly siltstone and sandstone.  Geological Province: Ashburton Basin.||||||07-NOV-08
698|Ashburton Formation|50380|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Wyloo Group.  Age: <184Ma.  Geological Province: Ashburton Basin||||||07-NOV-08
698|Ashburton Formation|60301|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Age: c. 1806Ma. Of the Wyloo Group. Geological Province: Ashburton Basin. Metamorphosed siltstone, lithic quartz sandstone, conglomerate and felsic volcanics.||||||17-AUG-04
698|Ashburton Formation|61262|5|Briefly described|p444|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group. Rocks of the Morrisey Metamorphic Suite grade into this unit. Consists of a thick sequence of turbitditic siliciclastic rocks of deep marine orgin. Age: ca1830-1800Ma (Evans et al 2003; Sircombe 2003).||||||07-NOV-08
698|Ashburton Formation|61270|6|Mentioned|p95|||||||||
698|Ashburton Formation|61276|4|Described|p577-580|Orosirian|Orosirian|Of the Wyloo Group. Overlies the Duck Creek Dolomite. Includes bi-modal volcanic sequence dated at  1829 +/- 5Ma (Volcanics).||||||17-OCT-16
698|Ashburton Formation|61526|5|Briefly described|p880|||Of Upper Wyloo Gp. Includes Mininer Turbidite Member and Wandarry Shale. Consists of turbidites; basal part comprises clastics, sandy BIF's and carbonates which are unconformable or disconformable on June Hill Volcanics. Geol. Prov: Ashburton Basin.||||||
698|Ashburton Formation|62129|3|Fully described|p1, p13, p16, p18|Proterozoic|Proterozoic|Of Wyloo Group. Comformably underlain by Duck Creek Dolomite. Thick: 12000m. Geol Prov: Ashburton Basin. Feldspathic and lithic quartz sandstone, interbedded with variable amounts of argillite and minor conglomerate. See p16 for more information.||||||07-FEB-11
698|Ashburton Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Thin- to thick-bedded metasandstone, pelite and local metaconglomerate.||||||23-DEC-09
698|Ashburton Formation|63246|5|Briefly described|p478 Fig. 1|||Of the Wyloo Group.||||||
698|Ashburton Formation|63866|4|Described|p154, p168|Statherian|Orosirian|SHRIMP ages derived from GSWA 148922.|1806 +/- 9 Ma (SHRIMP, U-Pb zircon)|||Overlies the June Hill Volcanics. Intruded by the Boolaloo Granodiorite.|Volcaniclastic sandstone and siltstone.|
698|Ashburton Formation|63869|4|Described|p5-7, p10, p14-15, p28, p45, p51, p53-54|Paleoproterozoic|Paleoproterozoic|See also p55-56, Plate 1. SHRIMP U-Pb zircon from a pumice-breccia sandstone. Older ages obtained by Sircombe (2002, 2003) and others are given. The contradictory ages may be due to markedly diachronous sedimentation during the Capricorn Orogeny. 5-12 km thick. Deformation and metamorphism discussed. Host to Au, Cu, Pb and Ag in quartz veins, and Au in alluvial/colluvial overlying deposits.|1806 +/- 9 Ma (GSWA, 2005).|Topmost unit in Wyloo Group.||Conformably overlies Duck Creek Dolomite and June Hill Volcanics. Is intruded by Boolaloo Granodiorite. Is overlain unconformably by the Capricorn, Bresnahan and Edmund Groups.|Mudstone and siltstone (65% of the Formation) and immature sandstone (30%), interbedded with minor conglomerate (clast- and matrix-supported) and felsic volcaniclastic rock; metamorphosed to pelitic, semi-pelitic and psammitic schists.|
698|Ashburton Formation|64287|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
698|Ashburton Formation|64384|5|Briefly described|p47 Tb. 7|||Top unit of Wyloo Group. Conformable on Duck Creek Dolomite. Geological province: Ashburton Basin. Mudstone and immature sandstone interbedded with a small amount of conglomerate, BIF and chert, and felsic to mafic volcanics.||||||07-FEB-11
698|Ashburton Formation|64728|6|Mentioned|p97, pp106-107.|||Mentioned as a potential source rock for Bangemall Supergroup.|Depositional age is c.1800 Ma.|Unit in upper Wyloo Group.||||
698|Ashburton Formation|64872|6|Mentioned|p24 Fig.1|||Unit in Wyloo Group.||||||
698|Ashburton Formation|65152|6|Mentioned|p2 Fig.1.|||Unit in Wyloo Group.||||||
698|Ashburton Formation|65830|3|Fully described|p3, p4, p10, p12-14, p24-26, Plate 2|Orosirian|Orosirian|Age from a felsic volcaniclastic sandstone. Other ages include c.1819 Ma (zircons in sandstone: Sircombe, 2002) and 1829 +/- 5 Ma (SHRIMP: volcaniclastic unit: Sircombe, 2003). Interpreted by Thorne and Seymour (1991) as a linear submarine fan system developed in a foreland basin.|1806 +/- 9 Ma (SHRIMP U-Pb zircon: GSWA, 2006),  |Of the Wyloo Group.||Underlain by the June Hill Volcanics. Unconformably overlain by the Capricorn Group, Irregully Formation, Bangemall Supergroup. Intruded by the Boolaloo Granodiorite.|Composed of mudstone, siltstone and immature sandstone, interbedded with minor amounts of conglomerate, and felsic and mafic volcanic rocks.|
698|Ashburton Formation|66115|5|Briefly described|p136-138|Paleoproterozoic|Paleoproterozoic|||Wyloo Group||Conformably overlies Duck Creek Dolomite (southwestern portion in core of Duck Creek Syncline).|Mudstones and iron formation (two iron formations are below in Duck Creek Dolomite); sub-greenschist metamorphism.|
698|Ashburton Formation|66299|5|Briefly described|p3, p121, pp202-205.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Thought to pass, with increasing metamorphic grade, into the Leake Spring Metamorphics to the south. Subjected to three stages of deformation. D2 produced faults and subparallel quartz veins, locally mineralised.|>1805 Ma.|Unit in Wyloo Group.||Is overlain unconformably by Capricorn Group.||
698|Ashburton Formation|66887|5|Briefly described|p2|||Ashburton Basin.||Wyloo Group, upper|||Low-grade metasedimentary rocks.|
698|Ashburton Formation|66950|5|Briefly described|p4, p10 Fig.9, p11, p15, p18, p23, p25|Orosirian|Orosirian|Gascoyne Province.|c. 1830-1800 Ma|Of the Wyloo Group.||Intruded by the Moorarie Supersuite. Cross-cut by the Boolaloo Granodiorite. Overlain unconformably by the Capricorn Group.|Comprises two distinct parts - a lower package of deep marine turbidites derived from a source to the southeast of the basin, overlain by turbidites deposited in prograding fans.|15-DEC-16
698|Ashburton Formation|67025|6|Mentioned|p319.|Paleoproterozoic|Paleoproterozoic|||Topmost unit in Wyloo Group.||||
698|Ashburton Formation|67056|5|Briefly described|p419 Fig.2. |Paleoproterozoic|Paleoproterozoic|||Unit in Upper Wyloo Group.||Overlies June Hill Volcanics.||
698|Ashburton Formation|67130|5|Briefly described|p3 fig 2, p5, p24 fig 17, p25|Statherian|Orosirian|5-10km  thick, deposited primarily in a deep water setting. Age is of deposition.|1829 Ma - 1795 Ma|Wyloo Group, Upper||Conformably overlies Duck Creek Dolomite, Interbedded with June Hill Volcanics, Unconformably overlain by Bangemall Group|Sandstone, siltstone and mudstone with subordinate conglomerate, banded iron formation and felsic to mafic volcanics.|
698|Ashburton Formation|67136|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|c.1806 Ma.|Unit in Wyloo Group.||In cross-section, underlies Bresnahan Group.|Siltstone, thin- to very thick-bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist facies (section only).|14-NOV-11
698|Ashburton Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.|c.1806 Ma.|Unit in Wyloo Group.|||Siltstone, thin- to very thick-bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rocks; lower greenschist facies.|
698|Ashburton Formation|67843|6|Mentioned|p3. |||||Unit in Wyloo Group.||||
698|Ashburton Formation|67855|4|Described|p216-9, 210, 212,229, 232, 198|Paleoproterozoic|Paleoproterozoic|Probably 5-10km , but too complex to be sure. Three facies present: Lowest 50-500m is basin-plain (grading from Duck Creek Dolomite). Then 1-2km of interchannel and basin-plain, then 3-6km of interchannel mudstone. Multichannel facies conglomerates, massive sandstones exist in units 25-225m thick.||Top of Wyloo Group.||Conformable over Duck Creek Dolomite. Unconformable over Fortescue Group. Disconformable over June Hill Volcs. Unconformably overlain by Capricorn, Mount Minnie Fms, Bangemall, Bresnahan Groups.|Mudstone and immature sandstone interbedded with minor amounts of conglomerate, BIF and felsic to mafic volcanics.|
698|Ashburton Formation|67888|6|Mentioned|p52|||||Wyloo Group||||
698|Ashburton Formation|68035|4|Described|p293, 294, p292 fig 6|Statherian|Orosirian|Ashburton Basin. Relatively deep-water sedimentary and volcanic rocks, >5 km thick. Includes Au deposits in quartz veins.|1829-1795 Ma|Of upper Wyloo Group.||Conformably overlies Duck Creek Dolomite. ?intruded by June Hill Volcanics, or lateral equivalent? Unconformably overlain by Bangemall Group.|Sandstone, siltstone.|
698|Ashburton Formation|68280|5|Briefly described|p5, p54|Paleoproterozoic|Paleoproterozoic||1829-1806 Ma|||Overlies Duck Creek Dolomite, intruded by June Hill Volcanics|Sandstone and siltstone.|
698|Ashburton Formation|68285|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton Basin. Shown as pre-dating Capricorn Orogeny (1817-1722 Ma, Evans 2003, AJES).|c. 1806 Ma|Of the Wyloo Group.||Unconformably overlain by Bresnahan Group or Irregully Formation, Edmund Group.|Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist facies (section only).|
698|Ashburton Formation|68286|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton Basin. Shown as pre-dating Capricorn Orogeny (1817-1722 Ma, Evans 2003, AJES)|c. 1806 Ma|Of the Wyloo Group.||Unconformably overlain by the Irregully Formation, Edmund Group.|Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock; lower greenschist facies (section only).|
698|Ashburton Formation|68981|5|Briefly described|p20-22|||Evans et al. (2003). Ashburton Basin. Deposition associated with the 1820-1770 Ma Capricorn Orogeny. Sediments supplied from the SE (Gascoyne Province).|c.1800 Ma.|Wyloo Group.||||
698|Ashburton Formation|69003|4|Described|p24-26|Paleoproterozoic|Paleoproterozoic|Ashburton Basin, Capricorn Orogen. Deep-marine deposits.|1830-1800 Ma.|Wyloo Group.||Overlies Duck Creek Dolomite. Is overlain unconformably by Capricorn Group.|Thick succession of turbidites, sandstone and conglomerate, interbedded with mudstone in upper part of the Formation.|
698|Ashburton Formation|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Age constrained by the Wyloo Group. 3 unnamed sub-units and metamorphosed Ashburton Formation schists are also mapped separately; see map legend for detailed lithologies.||Of the Wyloo Group.||Overlain by the Bywash Formation.|Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock, lower greenschist facies.|05-MAY-14
698|Ashburton Formation|69027|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton Basin. Geochronology by Hall et al. (2001); GSWA (in prep); and Sircombe (2003).|1829-1806 Ma |Of the Wyloo Group.||Overlain by the Yilgatherra Formation.|Siltstone, thin to very thick bedded lithic quartz sandstone, pebble to cobble conglomerate, and felsic volcanic rock (lower greenschist facies); interbedded psammite and pelite, including schists (Section only).|05-MAY-14
698|Ashburton Formation|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. Mapped with Duck Creek Dolomite and Mount McGrath Formation as a single unit.||Of the Wyloo Group, upper.|||Wacke, mudstone, ferruginous mudstone, banded iron-formation, chert, sandstone, conglomerate, felsic and mafic volcanic rocks, and locally stromatolitic dolomite.|07-MAY-14
698|Ashburton Formation|69080|5|Briefly described|p688, p691-694, p697 Fig.11|||Age from a tuffaceous unit.|c.1829 Ma (Sircombe, 2003).|Unit in Wyloo Group.||Overlies Duck Creek Dolomite. Is overlain unconformably by Capricorn Group.||
698|Ashburton Formation|69166|4|Described|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Age derived from sample of fine grained volcaniclastic rock (148922.1.pdf)|1806 Ma +/- 9Ma (SHRIMP) |Wyloo Group|||Basaltic pillow lava and pillow breccia, volcaniclastic sandstone and siltstone, interbedded psammite and pelite; schist, lithic quartz sandstone, pebble to cobble conglomerate, pebbly sandstone; lower greenschist facies.|
698|Ashburton Formation|69237|5|Briefly described|p1-2|Paleoproterozoic|Paleoproterozoic|Overlies the northern Gascoyne Province.||Wyloo Group.||||
698|Ashburton Formation|69538|6|Mentioned|p517 Fig.3|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.||||
698|Ashburton Formation|69546|6|Mentioned|p102|Paleoproterozoic|Paleoproterozoic|Geological province: Gascoyne Province.||||||
698|Ashburton Formation|69596|6|Mentioned|p6|||Pilbara Craton.||||||
698|Ashburton Formation|69754|6|Mentioned|p330-p331, p333|||Pilbara Craton.|c. 1800 Ma|Wyloo Group|||Banded-iron formation.|
698|Ashburton Formation|70327|6|Mentioned|p3|||||Wyloo Group.||||
698|Ashburton Formation|70767|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Section only: no outcrop in map area.|2008-1786 Ma.|Wyloo Group.||Is overlain unconformably by Bresnahan Group.|Mudstone, siltstone and thin- to very thick-bedded lithic-quartz sandstone; minor pebble- to cobble-conglomerate, felsic to mafic volcanic rocks, BIF and dolostone. Lower greenschist facies.|
698|Ashburton Formation|70768|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Section only: no outcrop in map area.|2008-1786 Ma.|Wyloo Group.||Is overlain unconformably by Bresnahan Group.|Mudstone, siltstone and thin- to very thick-bedded lithic-quartz sandstone; minor pebble- to cobble-conglomerate, felsic to mafic volcanic rock, BIF and dolostone. Lower greenschist facies.|
698|Ashburton Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv,148922.1.pdf, West Australian Craton, Ashburton Basin|1806-1799 Ma|Wyloo Group||Unconformably overlain by Bywash Formation|Sandstone, siltstone, mudstone, conglomerate, dolostone and mafic and felsic volcanic rocks; metamorphosed.|
698|Ashburton Formation|70814|6|Mentioned|p73|||||Wyloo Group||||
698|Ashburton Formation|70949|5|Briefly described|p988-989|Paleoproterozoic|Paleoproterozoic|||Wyloo Group.|||Mudstone, siltstone, wacke, conglomerate.|
698|Ashburton Formation|70958|4|Described|p5-7, Fig. 1|Paleoproterozoic|Paleoproterozoic|In Ashburton Trough.||Of Wyloo Group.|Includes Wandarry Shale Member, Capricorn Member,  Mininer Turbidite Member.||Includes silty shale, rare thin white flinty tuffaceous bands.|
698|Ashburton Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, crystalline dolostone/dolomite, mudstone, basalt, volcanic breccia|
698|Ashburton Formation|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. Six facies are mapped separately.|c.1796 Ma.|Wyloo Group.|||Mudstone, siltstone, and thin- to very thick-bedded lithic quartz sandstone; minor pebble to cobble conglomerate, felsic to mafic volcanic rock, BIF and dolostone, lower greenschist facies.|
698|Ashburton Formation|71808|6|Mentioned|p149|||||Wyloo Group, Upper||||
698|Ashburton Formation|71869|6|Mentioned|p3|||Capricorn Orogen.|1805-1800 Ma|Wyloo Group||||
698|Ashburton Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Ashburton Basin. This unit and two informal unnamed sub-units listed.||Wyloo Group|||Mudstone, some ferruginous; siltstone and thin- to very thick-bedded lithic quartz sandstone; minor pebble- to cobble-conglomerate, felsic to mafic volcanic rock, banded iron-formation, chert and dolostone; lower greenschist facies.|
698|Ashburton Formation|72570|6|Mentioned|p3 fig 1|||||Wyloo Group||||
698|Ashburton Formation|72712|5|Briefly described|p3, p25, p34, p9, p49, p53.|Statherian|Orosirian|Of de la Hunty (1965).||Wyloo Group|Includes Wandarry Shale, Capricorn Member and Mininer Turbidite Member.|Disconformably overlies Duck Creek Dolomite.|Includes shale and greywacke.|
698|Ashburton Formation|72758|4|Described|p4 Fig.1, p9-12 Tb.1, p30-31.|Paleoproterozoic|Paleoproterozoic|Estimated to be 5-10 km thick, but structural complexity and lack of marker horizons make measurement impossible. Intruded by Boolaloo Granodiorite (c. 1680 Ma Rb-Sr). Submarine-fan and associated basin-plain sediments. Includes olistostromes and large exotic blocks. Affected by regional metamorphism E of Parry Range. See also p35-40, p43, p48, p54-55, p57-59.|min. age from intruding granite 1680 Ma|Wyloo Group||Conformably overlies Duck Creek Dolomite. Disconformably overlies June Hill Volcanics. Overlies Fortescue Group. Unconformably overlain by Mount Minnie, Bangemall Groups, Phanerozoic rocks.|Mudstone and immature sandstone interbedded with small amounts of conglomerate, BIF, and felsic to mafic volcanics. Conglomerate, wacke, mudstone, ferruginous mdstone, minor chert.|
698|Ashburton Formation|73102|5|Briefly described|p3|||Pilbara Craton.|||||Mudstone, siltstone and lithic quartz sandstone; minor conglomerate, felsic to mafic volcanic rock, banded iron-formation, and dolostone; lower greenschist facies.|
718|Ashmore Volcanics|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60, p403|Late Jurassic|Late Jurassic|Type Section: Ashmore Reef 1 well (2469-2787m). 317m thick.||||Overlies Sahul Group (disconformably),|Altered basalt flows and claystone.|
718|Ashmore Volcanics|34363|6|Mentioned|p56|Late Jurassic|Late Jurassic|See p58, Fig.7. Oxfordian.||||||18-JUL-06
718|Ashmore Volcanics|41532|4|Described|p305|||||||||
718|Ashmore Volcanics|42442|3|Fully described|p25|Middle Jurassic|Early Jurassic|Age: Minimum of K/Ar 137 +/- 3 Ma? (does not conform with stated max/min age range).||||||18-JUL-06
718|Ashmore Volcanics|43699|6|Mentioned|Fig.6,p10||Late Jurassic|||||||
718|Ashmore Volcanics|49637|5|Briefly described|Fig. 3|Late Jurassic|Late Jurassic|Geological Province: Ashmore Platform.||||||07-FEB-11
718|Ashmore Volcanics|62837|5|Briefly described|Stratigraphic columns|Neocomian|Late Jurassic|Age: ~144-~133Ma. Geological Province:  Ashmore Platform.||||||01-MAR-10
718|Ashmore Volcanics|65708|6|Mentioned|p97|||Browse Basin. ~700m thick.|||||Subaerial volcanics and volcaniclastics.|
718|Ashmore Volcanics|69297|6|Mentioned|p305|Bathonian|Hettangian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Troughton Group||Overlies the Nome Formation. Unconformably overlain by the Montara Formation.||
718|Ashmore Volcanics|69452|5|Briefly described|p36:15|Early Cretaceous|Jurassic|Ashmore Platform, Bonaparte Basin.||Troughton Group.||||12-JUL-16
718|Ashmore Volcanics|70061|6|Mentioned|Regional geology Fig.7|Tithonian|Hettangian|Shown as a unit in both Troughton and Swan Groups.||Troughton Group.||||12-JUL-16
718|Ashmore Volcanics|70064|5|Briefly described|Regional: Fig. 6. Central: Fig.2|Bathonian|Hettangian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Troughton Group.||Overlies Nome Formation (Sahul Group). Is overlain by Lower Vulcan Formation or Montara Formation (Swan Group).||
723|Asterias Member|42053|5|Briefly described|Fig.3 p30|||||||||28-APR-16
735|Athol Formation|12491|5|Briefly described|p453-456.|Middle Jurassic|Early Jurassic|Exmouth Sub-basin. Rifting initiated during Pliensbachian forming a major depocentre.||||Overlies Murat Formation. Is overlain by Calypso Formation.|Monotonous sequence of silty shales deposited in low-energy, marine setting with restricted circulation.|03-NOV-14
735|Athol Formation|12498|6|Mentioned|p517 Fig.3. |Middle Jurassic|Early Jurassic|||||||
735|Athol Formation|13615|6|Mentioned|p82|||||||||
735|Athol Formation|14227|5|Briefly described|p10, p11|Aalenian|Pleinsbachian|Geological Province: Exmouth Sub-basin. Marine sedimentation including shales.||||||07-FEB-11
735|Athol Formation|22702|5|Briefly described|p105||Middle Jurassic|||||||
735|Athol Formation|23379|5|Briefly described|p164||Middle Jurassic|Of Barrow Sub-basin, Carnarvon Basin.||||||01-SEP-08
735|Athol Formation|23726|5|Briefly described|p8 Fig 2c|Middle Jurassic|Early Jurassic|Overlying unit Dingo Claystone. Underlying unit Murat Siltstone. Geological Province: Carnarvon Basin.||||||
735|Athol Formation|24084|5|Briefly described|p146 Fig.2|Middle Jurassic|Early Jurassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
735|Athol Formation|24246|5|Briefly described|p18, 19|Middle Jurassic|Early Jurassic|Geological Province: Carnarvon Basin.||||||
735|Athol Formation|24351|5|Briefly described|Plate 4 (in pocket)|Middle Jurassic|Early Jurassic|Geological Province: Exmouth Sub-basin.||||||13-DEC-07
735|Athol Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
735|Athol Formation|41732|6|Mentioned|p534|||||||||
735|Athol Formation|41751|2|Defined|p4|Toarcian|Bathonian|||||||
735|Athol Formation|42116|5|Briefly described|Fig.1 P6|||||||||
735|Athol Formation|42615|1|Redefined|p29|Pliensbachian|Pliensbachian|Age: Early Jurassic (late Pliensbachian).||||||01-SEP-08
735|Athol Formation|42822|5|Briefly described|p110|||||||||
735|Athol Formation|43826|6|Mentioned|Fig.2,p163||Middle Jurassic|||||||01-MAR-10
735|Athol Formation|44937|5|Briefly described|p92-3||Early Jurassic|||||||
735|Athol Formation|44938|4|Described|p151, Fig.3||Bathonian|||||||
735|Athol Formation|50024|5|Briefly described|p13|Early Jurassic|Early Jurassic|Geological Province: Carnarvon Basin.||||||
735|Athol Formation|50085|5|Briefly described|p23 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin.||||||
735|Athol Formation|60379|6|Mentioned|p126 fig 3, p136, p138|Middle Jurassic|Early Jurassic|Dampier sub-basin, Carnarvon Basin||||||
735|Athol Formation|60384|6|Mentioned|p244, p243 Fig 2b|Middle Jurassic|Late Triassic|Exmouth Sub-basin, Northern Carnarvon Basin.||||||
735|Athol Formation|60386|6|Mentioned|p300, 302|Middle Jurassic|Early Jurassic|Northern Carnarvon Basin. Proximal shelf and distal shelf/basin.||||||
735|Athol Formation|61023|5|Briefly described|p27 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin.||||||10-APR-08
735|Athol Formation|62734|5|Briefly described|p1362 Fig. 2|Middle Jurassic|Early Jurassic|Geological Province: Barrow Sub-basin.||||||10-APR-08
735|Athol Formation|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Early Jurassic|Age: ~190-165Ma. Geological Province: Northern Carnarvon Basin.||||||01-MAR-10
735|Athol Formation|63950|5|Briefly described|p336 Fig. 4, P337|Late Jurassic|Early Jurassic|Overlies Murat Siltstone; underlies and interfingers with Legendre and Learmonth Formations. Geological Province: northern Carnarvon Basin.Contains deep marine deposits of claystones.||||||01-FEB-10
735|Athol Formation|64978|6|Mentioned|p528 Fig.2.|Middle Jurassic|Early Jurassic|||||||
735|Athol Formation|66126|6|Mentioned|p206|Middle Jurassic|Middle Jurassic|Carnarvon Basin.||||||
735|Athol Formation|67200|5|Briefly described|p8 fig 6, |Jurassic|Jurassic|||||Overlies Murat Siltstone, Overlain by Biggada Formation, Dingo Claystone|Siltstone and some limestone.|
735|Athol Formation|67368|5|Briefly described|p209 Fig.4.|Middle Jurassic|Early Jurassic|Thick basin fill; seal.||||Overlies Murat Siltstone. Is overlain by Legendre Formation.||
735|Athol Formation|67369|6|Mentioned|p246 Fig.3. ||Early Jurassic|Dampier Sub-basin. Shown as Murat-Athol Fm. on the diagram for reasons of space.||||||
735|Athol Formation|67970|5|Briefly described|p25 Fig.4.|Bathonian|Toarcian|Exmouth Plateau.||||Overlies Murat Siltstone.||
735|Athol Formation|68135|5|Briefly described|p51 Fig.2a|Bathonian|Pliensbachian|Northern Carnarvon Basin.||||Overlies Murat Siltstone. Is overlain by Legendre and Calypso Formations.||14-SEP-17
735|Athol Formation|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13, Ch3 p23|||Carnarvon Basin. See also Ch3 p35, Ch3 p65-p66, Ch3 p73.||||||
735|Athol Formation|69297|6|Mentioned|p339, p352|Middle Jurassic|Middle Jurassic|Northern Carnarvon Basin.  Potential gas-prone source rock and seal. ||||||
735|Athol Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Northern Carnarvon Basin.||||Overlies Legendre Formation. Is overlain by Murat Siltstone.||
735|Athol Formation|69692|6|Mentioned|p4|Late Jurassic|Early Jurassic|Northern Carnarvon Basin.||||Overlies Murat Siltstone. Is overlain by Calypso Formation.||
735|Athol Formation|70065|6|Mentioned|Regional: p5|Jurassic|Jurassic|Northern Carnarvon Basin.||||||
735|Athol Formation|70066|5|Briefly described|Dampier: Fig.2;p1,p3. Exmouth: Fig.2; p2|Callovian|Toarcian|See also Regional: Fig.6; p5, p8-9. Northern Carnarvon Basin. Gas source from fluvio-deltaic sediments; marine to marginal marine sediments are a potential seal. Intra-formational claystones have the potential to form stacked reservoirs.||||Overlies Murat Siltstone. Is overlain by Legendre Formation.|Restricted marine claystone and siltstone.|
735|Athol Formation|70906|5|Briefly described|p757|Jurassic|Jurassic|Gorgon Platform.||||Overlies Murat Siltstone. Is overlain by Dingo Claystone.||
735|Athol Formation|73564|5|Briefly described|p1223, 1225|Jurassic|Jurassic|Exmouth Plateau, Gascoyne Margin.||||Overlies Murat Siltstone. Is overlain by Dingo Claystone.|Shallow- to deep-marine clastic sediments.|
744|Attlee Jaspilite Member|30562|4|Described|p38|Archean|Archean|Of Noganyer Formation||||||27-NOV-09
744|Attlee Jaspilite Member|43162|6|Mentioned|6|||||||||
762|Augusta Anorthosite Complex|24542|5|Briefly described|p18|||Includes garnet bearing hornblende-plagioclase gneiss, garnet anorthosite, layered anorthosite comprising anorthosite, leucogabbro and gabbro (metamorphosed to amphibolite), and mottled anorthosite.||||||
762|Augusta Anorthosite Complex|42069|4|Described|p241|||||||||
762|Augusta Anorthosite Complex|44138|5|Briefly described|p269|||Lithology details provided pp 269-270.||Leeuwin Complex|||Anorthosite or leucogabbro, mostly over 80% bytownite-labradorite; less than 20% hornblende, orthopyroxene and biotite.|
772|Austin Formation|23815|5|Briefly described|p278|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Basal unit of the Lyons Group.||||||13-DEC-04
772|Austin Formation|32648|6|Mentioned|p32|||In Lyons Group.||||||
772|Austin Formation|36890|6|Mentioned|p279|||||||||
772|Austin Formation|37295|6|Mentioned|Table 2|||||||||
772|Austin Formation|41271|6|Mentioned|p65|||||||||
772|Austin Formation|43566|6|Mentioned|p418|Sakmarian|Asselian|||||||
772|Austin Formation|44344|14|Not recorded|p.22,24,opp.4,map||Permian|Basal fm of Lyons Group. (G50-1). p.5-7||||||
772|Austin Formation|44345|14|Not recorded|map legend||Sakmarian|||||||
772|Austin Formation|45015|5|Briefly described|p53 Fig. 21, map legend|Permian|Permian|Of the Lyons Group. Age is Sakmarian. Probably supersedes  Austin Greywacke, but both names used in text. Geological Province: Carnarvon Basin.||||||29-JAN-08
772|Austin Formation|45016|2|Defined|p21-28||Sakmarian|Tb. at back, p.7,9-13,16,35,59,Fig.48. (G50-1 type section).||||||
772|Austin Formation|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
787|Auvergne Group|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, minor carbonate.||||||
787|Auvergne Group|9538|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone; minor dolomite.   Age: <900Ma.||||||
787|Auvergne Group|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||||||
787|Auvergne Group|14019|4|Described|p16, 29|Neoproterozoic|Neoproterozoic|Contains seven formations. Sandstone, siltstone, dolostone, conglomerate, dolarenite. Unconformably overlies Wattie Group. Age: 810-750Ma (Walter et al 1995, Thorne et al 1999). Geological Province: Victoria Basin.||||||11-APR-12
787|Auvergne Group|22547|6|Mentioned|p24|||Geological province: Victoria River Basin.||||||14-NOV-06
787|Auvergne Group|22809|6|Mentioned|Map|Proterozoic|Proterozoic|||||||
787|Auvergne Group|23216|6|Mentioned|Fig3p5||Mesoproterozoic|||||||
787|Auvergne Group|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Victoria Basin.  Correlates with Helicopter Sandstone, Ahern Formation (Victoria Basin), Renner Group (Ashburton Province) and the Roper Group (McArthur Basin).||||||09-NOV-04
787|Auvergne Group|23937|6|Mentioned|p23|||Correlated with the Roper Group.||||||
787|Auvergne Group|24122|3|Fully described|p9, p5 Tb.1|Proterozoic|Proterozoic|Includes Pinkerton Sandstone, Saddle Creek Formation, Angalarri Siltstone and Jasper Gorge Sandstone.  Geological Province: Victoria Basin.||||||25-JAN-10
787|Auvergne Group|24297|4|Described|p15|Proterozoic|Proterozoic|Defined by Sweet et al (1974 c). Comprises seven units, however only Jasper Gorge Sandstone outcrops on VICTORIA RIVER DOWNS 1:250k.||||||
787|Auvergne Group|24298|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|||||||19-OCT-05
787|Auvergne Group|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin|||Includes Jasper Gorge Sandstone, Angalarri Siltstone, Saddle Creek Formation, Pinkerton Sandstone.|||14-MAR-18
787|Auvergne Group|24303|6|Mentioned|p59 Appendix|||Of the Victoria River Region. Possibly correlates with the Renner Group.||||||
787|Auvergne Group|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Unconformably overlies Tijunna Group. Geological Province: Victoria Basin.||||||07-JAN-09
787|Auvergne Group|24442|5|Briefly described|p50 Fig. 1|||Includes: Shoal Reach, Lloyd Creek, Saddle Creek Formations, Spencer, Pinkerton, Jasper Gorge Sandstones, and Angalarri Siltstone.   Geological Province: Victoria Basin.||||||
787|Auvergne Group|28255|4|Described|p62, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Overlain unconformably by Duerdin Group.||||||
787|Auvergne Group|29813|6|Mentioned|Table 2|||||||||
787|Auvergne Group|30003|4|Described|p7, p13|Adelaidean|Adelaidean|Comprises seven conformable formations of shale, siltstone, sandstone and dolomite. Total thickness: 915m. Unconformably overlain by Duerdin Group. Adelaidean.||||||22-MAY-08
787|Auvergne Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Adelaidean||||||
787|Auvergne Group|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
787|Auvergne Group|32172|4|Described|Table 1|||See also p9. Adelaidean.||||||18-JUL-06
787|Auvergne Group|32173|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Angalarri Siltstone and Jasper Gorge Sandstone.||||||16-NOV-04
787|Auvergne Group|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Jasper Gorge Sandstone and Stubb Formation.||||||02-DEC-04
787|Auvergne Group|32307|4|Described|Table 2|||Proterozoic||||||
787|Auvergne Group|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
787|Auvergne Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
787|Auvergne Group|32660|4|Described|Table 6|||||||||
787|Auvergne Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||02-DEC-04
787|Auvergne Group|32700|4|Described|Table 1|||See also p14||||||18-JUL-06
787|Auvergne Group|32701|4|Described|Table 1|||Adelaidean. See also p9.||||||18-JUL-06
787|Auvergne Group|32728|6|Mentioned|p16|||||||||
787|Auvergne Group|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Stubb Formation, Jasper Gorge Sandstone, Angalarri Siltstone, Saddle Creek Formation and the Pinkerton Sandstone.||||||02-DEC-04
787|Auvergne Group|33373|3|Fully described|p9|||Table 2.||||||
787|Auvergne Group|33374|5|Briefly described|p8|||Strat. table||||||
787|Auvergne Group|33375|6|Mentioned|p11 Tb. 1, p12|Adelaidean|Adelaidean|Originally sandstones and shales of this group were assigned to "Mount John Series" by  Wade (1924).||||||27-APR-05
787|Auvergne Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
787|Auvergne Group|33377|5|Briefly described|Table 2|||||||||
787|Auvergne Group|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||27-APR-05
787|Auvergne Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
787|Auvergne Group|37462|4|Described|Table 4.VI|||||||||
787|Auvergne Group|37579|5|Briefly described|Regional setting map legend|Adelaidean|Adelaidean|Siltstone, shale, sandstone, minor dolomite.||||||10-OCT-05
787|Auvergne Group|38157|6|Mentioned|p284|||||||||
787|Auvergne Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
787|Auvergne Group|39563|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
787|Auvergne Group|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
787|Auvergne Group|39801|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone; minor dolomite.||||||04-OCT-05
787|Auvergne Group|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
787|Auvergne Group|40105|6|Mentioned|Fig.3|||||||||
787|Auvergne Group|40168|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone, minor dolomite.||||||18-OCT-05
787|Auvergne Group|40223|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone, minor dolomite.||||||19-OCT-05
787|Auvergne Group|40494|4|Described|p11|||||||||
787|Auvergne Group|40495|6|Mentioned|p12|||||||||
787|Auvergne Group|40765|6|Mentioned|p11|||||||||
787|Auvergne Group|40823|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
787|Auvergne Group|41407|6|Mentioned|Map legend|Neoproterozoic||||||||
787|Auvergne Group|41586|6|Mentioned|Map legend|||||||||
787|Auvergne Group|41645|4|Described|p16|||||||||
787|Auvergne Group|41646|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Quartzarenite, flaggy, ripple marked, laminated, moderatly friable. Sandstone, siltstone, minor carbonate.||||||14-OCT-05
787|Auvergne Group|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Pinkerton Sandstone, Saddle Creek Formation and Angalarri Siltstone. Sandstone, siltstone, minor carbonate.||||||07-OCT-05
787|Auvergne Group|41661|5|Briefly described|p19|||Mention on P23||||||
787|Auvergne Group|42014|5|Briefly described|Map legend|Mesoproterozoic||||||||
787|Auvergne Group|43187|5|Briefly described|p2|||||||||
787|Auvergne Group|43561|6|Mentioned|p1441|||||||||
787|Auvergne Group|44155|6|Mentioned|p252|||Victoria River Basin.||||Part-correlative of upper Wade Creek Sandstone (Kimberley Basin).||
787|Auvergne Group|45112|5|Briefly described|Table 3|||||||||
787|Auvergne Group|45140|5|Briefly described|p13-14, p59|||Victoria River region. Lower part is correlated with upper Wade Creek Sandstone.|||Jasper Gorge Sandstone.|Is overlain by Duerdin Group.||
787|Auvergne Group|45162|6|Mentioned|p152|||||||||
787|Auvergne Group|46675|5|Briefly described|Map legend for regional setting...|Paleozoic|Neoproterozoic|Siltstone, shale, sandstone; minor dolomite.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
787|Auvergne Group|46864|6|Mentioned|Fig.4|||||||||
787|Auvergne Group|48938|2|Defined|p32|Adelaidean|Adelaidean|||||||
787|Auvergne Group|48942|3|Fully described|p61|||See also pp62-71.||||||18-JUL-06
787|Auvergne Group|48943|4|Described|p72|||||||||
787|Auvergne Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria River Basin.||||||07-FEB-11
787|Auvergne Group|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Sandstone, siltstone, dolostone, conglomerate, dolarenite.||||||
787|Auvergne Group|60526|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Siltstone, shale, sandstone, minor dolomite.||||||
787|Auvergne Group|60589|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Angalarri Sandstone and the Jasper Gorge Sandstone.  Sandstone, siltstone, dolostone, conglomerate, dolarenite.  Geological Province: Victoria Basin.||||||24-NOV-04
787|Auvergne Group|60672|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone. Geological Province: Victoria Basin.||||||11-JAN-05
787|Auvergne Group|60682|4|Described|piii|Cryogenian|Cryogenian|Unconformably overlies: Bullita Group. Age: 810-750Ma. Geological Province: Victoria Basin. Contains 7 formations. Thickness: 950m.||||||04-MAY-05
787|Auvergne Group|60685|5|Briefly described|p4 Figure 3, p1|Mesoproterozoic|Mesoproterozoic|Thickness: 950m. Sandstone, siltstone, dolostone, conglomerate, dolarenite. Unconformably overlies Wattie, Bullita and Tijunna Groups; unconforably overlain by Antrim Plateau Volcanics. Age: 1.57-1.35 Ga?, 810-750Ma?. Geol. Prov: Victoria Basin.||||||
787|Auvergne Group|61560|5|Briefly described|p490|Mesoproterozoic|Mesoproterozoic|Includes the Jasper Gorge Sandstone.  Geological Province: Victoria Basin. ||||||
787|Auvergne Group|61573|5|Briefly described|p676, p678 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes Angalarri Siltstone, Saddle Creek Formation and Pinkerton Sandstone. Overlies the Tijunna Group. Age: <1500Ma. Geological Province: Victoria Basin.||||||
787|Auvergne Group|63866|5|Briefly described|p108, p117||Stenian|Litchfield Province, Pine Creek Orogen.|c. 1050 Ma (maximum depositional age)|||Overlies the Fitzmaurice Group. Overlain by the Uniya Formation.||
787|Auvergne Group|64104|6|Mentioned|p75, p76 fig 10, p77|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Suggested source of sedimentary clasts in Duerdin Group in Keep River area. Age is from fig.10, p76.||||||18-MAY-15
787|Auvergne Group|64698|4|Described|lithinterp table|||Age stated to be 750-810Ma (Cryogenian), but age name given is Statherian. Victoria - Birrindudu Basin. Max thick 1900m. Sandstone, siltstone, shale, becomes more dolomitic to top of Auvergne Group.||||||10-FEB-10
787|Auvergne Group|64724|6|Mentioned|p49 Fig. 7|Cryogenian|Cryogenian|Deposited in the Victoria River Basin.||||||02-APR-12
787|Auvergne Group|65232|6|Mentioned|p5 Fig. 4|||Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
787|Auvergne Group|65331|5|Briefly described|Map legend + overview geology map legend|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Includes Shoal Reach Formation, Spencer Sandstone,  Lloyd Creek Formation, Pinkerton Sandstone, Saddle Creek Formation, Angalarri Siltstone, Jasper Gorge Sandstone. Sandstone, siltstone, dolostone, conglomerate, dolarenite||||||02-FEB-10
787|Auvergne Group|65339|6|Mentioned|p5 Fig.4. ||||||||Siltstone, shale, sandstone.|
787|Auvergne Group|65342|5|Briefly described|pp10-11.|||Victoria Basin.|||Includes Jasper Gorge, Pinkerton and Spencer Sandstones; Angalarri Siltstone; Saddle Creek, Lloyd Creek and Shoal Reach Formations.|Unconformably overlies Tijunna Group.|Sandstone, siltstone, evaporitic carbonate rocks.|
787|Auvergne Group|65417|6|Mentioned|p159.|||Victoria River Basin.|||Includes Angalarri Siltstone.|||
787|Auvergne Group|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.|||Includes Jasper Gorge and Pinkerton Sandstones; Angalarri Siltstone and Saddle Creek Formation.|Unconformably overlies Tijunna Group. Is unconformably overlain by Duerdin Group.||
787|Auvergne Group|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Areas with diferent magnetic responses are indicated.|||Includes Angalarri Siltstone; Saddle Creek and Lloyd Creek Formations; Pinkerton and Spencer Sandstones.|||
787|Auvergne Group|68733|5|Briefly described|p177-179, p181-186, p189, p191-193|Cryogenian|Cryogenian|Victoria Basin. The basal unconformity separates the Birrindudu and Victoria Basins.|c.830 Ma.||Includes Shoal Reach, Lloyd Creek, Saddle Creek Formations; Spencer, Pinkerton, Jasper Gorge Sandstones; Angalarri Siltstone.|Unconformably underlain by the Tijunna Group.||04-DEC-17
787|Auvergne Group|69422|6|Mentioned|p7:2 Fig.7.2|Neoproterozoic|Neoproterozoic|Victoria Basin.||||||12-JUL-16
787|Auvergne Group|69432|5|Briefly described|p17:1-2, 12|Neoproterozoic|Neoproterozoic|Victoria Basin. This study places the break between the Birrindudu and Victoria Basins at the base of this unit.|838 +/- 80 Ma.|||Unconformably overlies Tijunna Group.||12-JUL-16
787|Auvergne Group|69437|6|Mentioned|p22:6|||Victoria Basin. Poorly dated.||||||12-JUL-16
787|Auvergne Group|69441|4|Described|p26:1-6|Neoproterozoic|Neoproterozoic|Victoria Basin. 950m thick. Forms most of the Pinkerton, Spencer, Yambarra and Newcastle Ranges. Best estimate of age is 838 +/- 80 Ma for the Angalarri Siltstone. An inferred minimum age of c.635 Ma is based on correlations of the overlying Moonlight Valley Tillite. Affected by intense deformation in the 1 km-wide Victoria River Fault Zone. Carbonate and shale units are prospective for base metals. No petroleum shows were found in the Bullo River-1 core in 1984; there has been no subsequent exploration. Uranium exploration results are disappointing.|||Shoal Reach, Lloyd Creek, Saddle Creek Formations; Spencer, Pinkerton, Jasper Gorge Sandstones; Angalarri Siltstone.|Unconformably overlies Tijunna Group.||12-JUL-16
787|Auvergne Group|69442|5|Briefly described|p27:1-2, 3 Tb.27.1||||||Shoal Reach, Saddle Creek Formations; Spencer Sandstone; Angalarri Siltstone.|Is overlain unconformably by Big Knob beds, Moonlight Valley Tillite and Skinner Sandstone.||12-JUL-16
787|Auvergne Group|69445|5|Briefly described|p30:4|Proterozoic|Proterozoic|Victoria River region, Victoria Basin.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
787|Auvergne Group|69673|6|Mentioned|p48 fig 35, p187, p188|||950m thick.|||Includes Jasper Gorge Sandstone, Angalarri Siltstone, Saddle Creek Formation, Pinkerton Sandstonem Lloyd Creek Formation, Spencer Sandstone, Shoal Reach Formation|Unconformably overlies Tijunna Group||
787|Auvergne Group|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.|||Includes Shoal Reach Formation, Spencer Sandstone, Lloyd Creek Formation, Pinkerton Sandstone, Saddle Creek Formation, Angalarri Siltstone, Jasper Gorge Sandstone.|||
787|Auvergne Group|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin|||Includes Pinkerton Sandstone, Saddle Creek Formation, Angalarri Siltstone, Jasper Gorge Sandstone.|Unconformably overlies Tijunna Group, Wattie Group, Bullita Group. Is unconformably overlain by Duerdin Group, Kinevans Sandstone.||
787|Auvergne Group|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.|||Jasper Gorge, Pinkerton Sandstones; Angalarri Siltstone; Saddle Creek Formation.|Unconformably overlies Tijunna Group.||
787|Auvergne Group|70854|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.|||Jasper Gorge Sandstone.|Unconformably overlies Tijunna Group. Is overlain unconformably by Antrim Plateau Volcanics.||
787|Auvergne Group|70855|5|Briefly described|Map legend.|Neoproterozoic|Mesoproterozoic|Victoria Basin.|||Jasper Gorge Sandstone.|Unconformably overlies Bullita Group. Is overlain unconformably by Antrim Plateau Volcanics.||
787|Auvergne Group|70968|5|Briefly described|p115-117, p120, p124, p137|Neoproterozoic|Neoproterozoic|Victoria Basin.|||Jasper Gorge Sandstone, Angalarri Siltstone.|Unconformably overlies Tijunna Group.||
787|Auvergne Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, dolostone|
787|Auvergne Group|71302|5|Briefly described|p1-3,6, 43, 58,65,72,74-75|Neoproterozoic|Neoproterozoic|Of Victoria Basin. Major zircon provenance peaks at c. 1530-1600 Ma (maxima c. 1590 Ma) and c. 1050-1220 Ma coincide with Musgrave province magmatic events.|||Includes Shoal Reach Formation, Spencer Sandstone, Lloyd Creek Formation, Pinkerton Sandstone, Saddle Creek Formation, Angalarri Siltstone, Jasper Gorge Sandstone.|Overlain unconformably by Duerdin Group. Underlain unconformably by Tijunna Group.||09-DEC-19
787|Auvergne Group|71893|6|Mentioned|p69||||||Includes the Angalarri Siltstone.|||
787|Auvergne Group|73083|6|Mentioned|p30|Neoproterozoic|Neoproterozoic|Appears as uniform mid-grey on magnetic images.||||||
787|Auvergne Group|73255|6|Mentioned|p533 Fig.1|Tonian|Tonian|||||||
837|Babrongan Formation|40992|6|Mentioned|Fig.11|||||||||
837|Babrongan Formation|41751|6|Mentioned|p8|||||||||
837|Babrongan Formation|42030|5|Briefly described|p746|||||||||
837|Babrongan Formation|43818|6|Mentioned|Fig.2.p39||Late Devonian|||||||
837|Babrongan Formation|44143|4|Described|p.439 Table 4-19, p442|Devonian|Devonian|Up to 300m thick; shale and siltstone; marine. Type section between 1736 and 1949m in Babrongan 1 (MOUNT ANDERSON: 18deg 23' 23" S, 123deg 35' 37" E). Is overlain conformably by Clanmeyer Siltstone. Contains palynormorphs.||||||22-NOV-17
863|Badgeradda Group|14228|6|Mentioned|p4|Ordovician|Ordovician|Perry and Dickens (1960).||||||
863|Badgeradda Group|22716|6|Mentioned|p237|Mesoproterozoic|Mesoproterozoic|overlies northwestern margin of the Yilgarn Craton, may be equivalent to upper Bangemall Basin.||||||
863|Badgeradda Group|23569|4|Described|p4 Tb. 1|Proterozoic|Proterozoic|Comprised of the Yarrawolya, Coomberarie, Errabiddy and Woodrarrung Formations.||||||
863|Badgeradda Group|23574|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlying unit Lyons Group.||||||
863|Badgeradda Group|23576|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlying unit Lyons Group.||||||
863|Badgeradda Group|23577|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlying unit Lyons Group.||||||
863|Badgeradda Group|23816|6|Mentioned|p258|Proterozoic|Proterozoic|||||||
863|Badgeradda Group|24114|4|Described|p8|||Geological Province: Carnarvon Basin.||||||
863|Badgeradda Group|24410|5|Briefly described|p134 Fig. 79|Proterozoic|Proterozoic|Siltstone, shale, sandstone and dolomite.||||||24-NOV-09
863|Badgeradda Group|24526|5|Briefly described|p114, p106 Fig. 7|Neoproterozoic|Neoproterozoic|Comprises folded sandstone, shale and conglomerate. Age: >800Ma.  See also p112 Fig. 9.||||||
863|Badgeradda Group|24542|5|Briefly described|p2 Fig.2|Proterozoic|Proterozoic|Sandstone, shale and conglomerate.||||||
863|Badgeradda Group|29690|6|Mentioned|p12|||||||||
863|Badgeradda Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table.||||||
863|Badgeradda Group|30949|6|Mentioned|Map legend||Proterozoic|||||||
863|Badgeradda Group|36199|6|Mentioned|p1|||||||||
863|Badgeradda Group|36293|4|Described|p77|||||||||
863|Badgeradda Group|36551|6|Mentioned|p141|||||||||
863|Badgeradda Group|36872|3|Fully described|p71|||||||||
863|Badgeradda Group|37299|6|Mentioned|Fig.1|||||||||
863|Badgeradda Group|37344|6|Mentioned|p74|||||||||
863|Badgeradda Group|37460|4|Described|p177|||||||||
863|Badgeradda Group|38493|4|Described|p33|||||||||
863|Badgeradda Group|38494|4|Described|p25|||Formally Badgeradda Beds, Konecki et al 1958.||||||
863|Badgeradda Group|38766|6|Mentioned|Fig.2|||||||||
863|Badgeradda Group|38998|6|Mentioned|p3|||||||||
863|Badgeradda Group|40089|6|Mentioned|p12|||||||||
863|Badgeradda Group|40336|4|Described|p15|||||||||
863|Badgeradda Group|40339|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
863|Badgeradda Group|40340|5|Briefly described|p7|||||||||
863|Badgeradda Group|40341|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late||||||
863|Badgeradda Group|40342|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late||||||
863|Badgeradda Group|40343|4|Described|p3|||||||||
863|Badgeradda Group|40935|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
863|Badgeradda Group|41271|6|Mentioned|p8|||||||||
863|Badgeradda Group|42579|5|Briefly described|p12|||See also Table 2, Fig.3, Plate 1.||||||
863|Badgeradda Group|43255|5|Briefly described|map legend||Proterozoic|||||||
863|Badgeradda Group|43256|5|Briefly described|5,17||Proterozoic|||||||24-NOV-09
863|Badgeradda Group|43442|6|Mentioned|p41||Proterozoic|Underlies, but not considered part of, Carnarvon Basin Succession||||||
863|Badgeradda Group|43835|5|Briefly described|Map Legend||Proterozoic|||||||
863|Badgeradda Group|44138|6|Mentioned|p272||||||||Similar to the quartz greywacke and sandstone of the Nilling Formation, but less deformed and metamorphosed.|
863|Badgeradda Group|44142|4|Described|p328 Tb.4-5, p329|||Originally Badgeradda Beds (Konecki et al., 1958). Formations defined by Perry and Dickins (1960); Williams et al. (1983). Bordered by Darling Fault (to the W) and Meeberrie Fault (to the E). Unconformably overlies Western Gneiss Terrane.|||Includes Errabiddy and Woodrarrung Sandstones; Bililly, Coomberarie and Yarrawolya Formations.|Correlated with Bangemall Group.|Predominantly sandstone with lesser amounts of siltstone, shale and conglomerate; intruded by dolerite dykes.|13-MAR-18
863|Badgeradda Group|44532|14|Not recorded|p.5|||Equivalent not present.||||||
863|Badgeradda Group|45015|2|Defined|p18-24, map legend|Proterozoic|Proterozoic|Overlies Yarramulla Beds; unconformably overlain by Lyons Group. Contains: Nilling Beds, Bililly Formation, Errabiddy Sandstone, Woodrarrung Sandstone, Coomberarie Formation, Yarrawolya Formation (top). Geol. Prov: Carnarvon Basin.||||||19-AUG-14
863|Badgeradda Group|45016|14|Not recorded|p66|||(map).||||||
863|Badgeradda Group|45965|14|Not recorded|p.58|||||||||
863|Badgeradda Group|48823|5|Briefly described|p3 Tb. 1, map legend|Neoproterozoic|Paleoproterozoic|Formerly Badgeradda Beds. Includes: Bililly, Woodrarrung, Coomberarie and Yarrawolya Formations. Unconformably overlies Nilling Beds. Max. thickness: >10,000ft. See also p10 Tb. 2.||||||07-NOV-08
863|Badgeradda Group|61958|5|Briefly described|Map sheets 1 and 2|Neoproterozoic|Neoproterozoic|Includes Nilling Beds, Bililly Formation, Errabiddy Sandstone, Woodrarrung Sandstone, Coomberarie Formation and Yarrowolya Formation.||||||19-AUG-14
863|Badgeradda Group|62381|6|Mentioned|p2 Fig.2.|||||||||
863|Badgeradda Group|63866|6|Mentioned|p183|||||||||
863|Badgeradda Group|64580|6|Mentioned|map legend|||||||||
863|Badgeradda Group|64635|6|Mentioned|p2 Fig.1|||||||||
863|Badgeradda Group|64722|5|Briefly described|p20|||Predominantly siliciclastic strata with some volcanic and volcaniclastic rocks and minor dolomite lying adjacent to the Darling Fault.||||||
863|Badgeradda Group|65487|6|Mentioned|p2 Fig.1|||||||||
863|Badgeradda Group|69003|6|Mentioned|vi, p54-55, p72|||Yilgarn Craton. Appears as Badgeradda group on p55.||||||
863|Badgeradda Group|69080|6|Mentioned|p684|||Yilgarn Craton.|||||Sandstone; lesser siltstone and conglomerate.|
863|Badgeradda Group|69166|6|Mentioned|500k_geologyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Errabiddy Sandstone|||
863|Badgeradda Group|69387|6|Mentioned|p3|||||||||
863|Badgeradda Group|69583|4|Described|p131 Fig.2, p132-133, p134 Fig.3, p135|Neoproterozoic|Mesoproterozoic|See also p138, p141, p152, p156; Plates 2, 3, 4. Badgeradda Basin, Pinjarra Orogen. Part of the basement to the Southern Carnarvon Basin. Seismic interpretation. Unfossiliferous sedimentary rocks. Estimated thickness up to 3000m. Mis-spelt as Baggeradda Group on p135.|||Errabiddy, Yarrawolya Formations; Woodrarrung Sandstone.|Is overlain by Tumblagooda Sandstone.|Folded cross-bedded, coarse-grained, feldspathic quartz sandstone; shale; conglomerate.|
863|Badgeradda Group|70795|5|Briefly described|2_5m_interpgeop15_lut.csv|Neoproterozoic|Mesoproterozoic|500k_interpgeop14_lut.csv|1173-541 Ma||Includes Erabiddy Formation||Sandstone; lesser silstone and conglomerate.|
863|Badgeradda Group|70826|6|Mentioned|p5 tbl 2|||Centralian Superbasin.||||||20-APR-20
863|Badgeradda Group|71146|6|Mentioned|p16|Precambrian|Precambrian|Pinjarra Orogen.||||||
863|Badgeradda Group|72034|6|Mentioned|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Yarrawolya Formation, Coomberarie Formation, Woodrarrung Sandstone, Errabiddy Formation.|||
911|Baker Formation|14228|6|Mentioned|p8|Permian|Permian|||Byro Group||||
911|Baker Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
911|Baker Formation|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||23-DEC-09
911|Baker Formation|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
911|Baker Formation|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
911|Baker Formation|23726|5|Briefly described|p7 Fig 2b|Early Permian|Early Permian|Of Byro Group. Overlying unit Coolkilya Sandstone. Underlying unit Nalbia Sandstone. Geological Province: Carnarvon Basin.||||||
911|Baker Formation|23815|4|Described|p288|Kungurian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Minilya Subgroup. Overlying unit: Coolkilya Greywacke (disconformable). Underlying unit: Nalbia Greywacke. Max. thickness: 90m||||||18-APR-05
911|Baker Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
911|Baker Formation|30545|6|Mentioned|Fig.2|||Lower Permian||||||
911|Baker Formation|31561|6|Mentioned|p7|||||||||
911|Baker Formation|32648|6|Mentioned|p32|||Byro Gp.||||||
911|Baker Formation|33701|6|Mentioned|Fig.1|||Kungurian.||||||
911|Baker Formation|33710|6|Mentioned|p120|||Kungurian.||||||
911|Baker Formation|33711|6|Mentioned|p384|||See also Table 4.||||||
911|Baker Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
911|Baker Formation|34287|6|Mentioned|p142|||L.- M.Permian||||||
911|Baker Formation|34532|6|Mentioned|p225|||Byro Gp.||||||
911|Baker Formation|35282|6|Mentioned|p39|||||||||
911|Baker Formation|36020|6|Mentioned|p392|||||||||
911|Baker Formation|36257|6|Mentioned|Table 2.1|||||||||
911|Baker Formation|36740|5|Briefly described|p1|||||||||
911|Baker Formation|36890|3|Fully described|p288|||||||||
911|Baker Formation|37294|6|Mentioned|p103|||||||||
911|Baker Formation|37295|6|Mentioned|Table 2|||||||||
911|Baker Formation|37303|5|Briefly described|p65|||||||||
911|Baker Formation|37304|6|Mentioned|p55|||||||||
911|Baker Formation|37549|6|Mentioned|p109|||||||||
911|Baker Formation|39316|6|Mentioned|Fig.2|||||||||
911|Baker Formation|39974|6|Mentioned|p113|||||||||
911|Baker Formation|40617|6|Mentioned|Fig.1|||||||||
911|Baker Formation|41071|6|Mentioned|p29|||||||||
911|Baker Formation|41271|3|Fully described|p99|||Mention P90||||||
911|Baker Formation|41438|6|Mentioned|Fig.11|||||||||
911|Baker Formation|41632|6|Mentioned|p1|||||||||
911|Baker Formation|42116|5|Briefly described|p41|||||||||
911|Baker Formation|42392|6|Mentioned|p118|||Byro Group||||||
911|Baker Formation|42654|6|Mentioned|p10|||||||||
911|Baker Formation|42994|6|Mentioned|p62|||||||||
911|Baker Formation|43015|5|Briefly described|Table 1,p319|||||||||
911|Baker Formation|43050|5|Briefly described|p26|||||||||
911|Baker Formation|44219|14|Not recorded|p31||Artinskian|||||||
911|Baker Formation|44344|14|Not recorded|p.14-16,24|||?U.Artinskian; top fm in Minilya Subgroup in Byro Group. (G50-1). opp.4; map||||||
911|Baker Formation|44345|14|Not recorded|map legend||Artinskian|||||||
911|Baker Formation|44537|14|Not recorded|map legend||Artinskian|||||||
911|Baker Formation|44657|14|Not recorded|p.5,6,9,10|||||||||
911|Baker Formation|44994|6|Mentioned|Fig.7|||Perm. Correlation. Byro Gp.||||||
911|Baker Formation|45015|5|Briefly described|map legend|Late Permian|Late Permian|Of the Minilya Sub-Group (Byro Group). Geological Province: Carnarvon Basin.||||||31-MAY-06
911|Baker Formation|45016|2|Defined|p170-8||Artinskian|Tb. at back, p.124,125,155-157,163,165-7,180,181,184. (G50-14 -type area F50-13).||||||
911|Baker Formation|48610|14|Not recorded|Pl.1|||||||||
911|Baker Formation|48831|14|Not recorded|p.76|||||||||
911|Baker Formation|48858|14|Not recorded|p.5-15|||Absent from BMR No.6 bore. Pl.2||||||
911|Baker Formation|49644|5|Briefly described|Table|||||||||
911|Baker Formation|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of the Byro Group. Overlies Nalbia Sandstone. Overlain by Kennedy Group. Geological Province: Southern Carnarvon Basin.||||||
911|Baker Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||
911|Baker Formation|64580|5|Briefly described|map legend|||Of Upper Byro Group. Black shale to mudstone overlying fine-grained sandstone and shale.||||||15-DEC-08
911|Baker Formation|64974|6|Mentioned|p146|Kungurian|Kungurian|Geological Province: Carnarvon Basin.||||||24-JUN-09
911|Baker Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes reddish brown medium-grained sandstone.|
911|Baker Formation|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal conductivity of 3.51 W/mK. See also p47, p54, app 2 p5.||Byro Group||Overlies Nalbia Sandstone, overlain by Coolkilya Sandstone|Laminated siltstone beds, medium grained sandstone.|
911|Baker Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.|||Comprises siltstone and black shale; minor interbedded, fine-grained sandstone.|
911|Baker Formation|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
911|Baker Formation|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Wandagee Formation and Nalbia Sandstone.||Byro Group.|||Intercalated siltstone, shale and sandstone.|
911|Baker Formation|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group|||Siltstone and black shale; minor interbedded fine-grained sandstone.|
911|Baker Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, siltstone|
911|Baker Formation|72910|5|Briefly described|p10, p18, p23, p30, p38, p41.|Kungurian|Kungurian|Thickness 21 to 90m eroded in outcrop. Type section is located at North end of Kennedy Range, 24d13m30sS, 115d03m00sE. Said to be Artinskian age p38.||Top of Byro Group.||Conformably overlies Nalbia Sandstone underlies Coolkilya Sandstone.|Grey to black siltstone, sandy siltstone, silty fine sandstone. Sparsely fossiliferous including foraminifers and brachiopods.|
943|Bald Hill Granodiorite|40667|6|Mentioned|p193|||||||||
950|Baldwin Formation (WA)|32377|6|Mentioned|p226|||Major element chemistry||||||
950|Baldwin Formation (WA)|39560|6|Mentioned|p121|||||||||
1061|Banjan Creek Formation|37373|5|Briefly described|p78|||||||||
1088|Barbwire Sandstone|7433|5|Briefly described|p25 Fig.2, pp44-45. |Cretaceous|Jurassic|Canning Basin. Thin, fluvial, coarse clastics. Includes rocks formerly referred to as James Sandstone. Probably partly equivalent to upper Wallal Sandstone, Alexander Formation and Jarlemai Siltstone.|||||Well-rounded, pebble conglomerate, coarse sandstone; fluvial.|
1088|Barbwire Sandstone|22741|5|Briefly described|p30||Late Jurassic|||||||05-FEB-20
1088|Barbwire Sandstone|22753|5|Briefly described|Fig.3 p585|Jurassic|Jurassic|||||||
1088|Barbwire Sandstone|22767|5|Briefly described|Table3 p12, p23||Mesozoic|||||||05-FEB-20
1088|Barbwire Sandstone|22776|6|Mentioned|p11, Table.3|||Possible equivalent of the Meda Formation.||||||
1088|Barbwire Sandstone|41436|6|Mentioned|p46|||||||||
1088|Barbwire Sandstone|42613|6|Mentioned|P 18|||Includes the "James Sandstone".||||||
1088|Barbwire Sandstone|42930|5|Briefly described|Fig.1 p473|Jurassic|Jurassic|Lateral equivalent of Wallal Sandstone.  Geological Province: Canning Basin. Marine/deltaic deposits.||||||13-NOV-07
1088|Barbwire Sandstone|43563|6|Mentioned|Fig.2,p5||Late Jurassic|||||||
1088|Barbwire Sandstone|43656|6|Mentioned|Fig.2,p8|Tithonian|Callovian|||||||
1088|Barbwire Sandstone|43746|6|Mentioned|Fig.2,p11|Tithonian|Callovian|||||||
1088|Barbwire Sandstone|43818|6|Mentioned|Fig.2.p39|Late Jurassic|Early Jurassic|||||||
1088|Barbwire Sandstone|44403|2|Defined|p.8,9,10,11,12|||E/51-12, shale, calcarenous siltstone, limestone sandstone, intraformational conglomerate, marine fossils. Underlain disconformably by Poole Sandstone.||||||13-NOV-07
1088|Barbwire Sandstone|44404|14|Not recorded|map legend||Jurassic|||||||
1088|Barbwire Sandstone|44998|2|Defined|p143||Jurassic|Unconformably overlies Liveringa Formation. On many pages. 88,144-5,185,226.||||||
1088|Barbwire Sandstone|48938|2|Defined|p29|Proterozoic|Proterozoic|?Adelaidean.||||||
1088|Barbwire Sandstone|64580|4|Described|map legend||Jurassic|Sandstone, lesser conglomerate; minor siltstone.||||||17-NOV-08
1088|Barbwire Sandstone|64643|5|Briefly described|p3 Fig. 2|Late Jurassic|Middle Jurassic|||||||10-FEB-20
1088|Barbwire Sandstone|65301|5|Briefly described|p5 Fig. 4|Late Jurassic|Middle Jurassic|Geological province: Canning Basin.||||||23-FEB-10
1088|Barbwire Sandstone|65449|6|Mentioned|p6|Late Jurassic|Middle Jurassic|||||Is overlain by Alexander Formation. Lateral equivalent of Wallal Sandstone.||
1088|Barbwire Sandstone|68007|6|Mentioned|p4|Late Jurassic|Middle Jurassic|Canning Basin.||||||25-FEB-20
1088|Barbwire Sandstone|68902|6|Mentioned|p9 fig 5|Jurassic|Jurassic|||||Overlain by Alexander Formation||
1088|Barbwire Sandstone|69029|6|Mentioned|p319|Barremian|Berriasian|Of Canning Basin.||||Overlain by Broome Sandstone. Underlain by Jarlemai Siltstone.||
1088|Barbwire Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv||Jurassic||||||sandstone, lesser conglomerate; minor siltstone|
1088|Barbwire Sandstone|69165|4|Described|500k_geologyp08_lut.csv||||||||Sandstone, lesser conglomerate; minor siltstone.|
1088|Barbwire Sandstone|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p45|Jurassic|Jurassic|North Canning Basin.||||Overlain by the Alexander Formation.||
1088|Barbwire Sandstone|69297|6|Mentioned|p337, p352|Kimmeridgian|Oxfordian|Broome Platform of the Canning Basin. ||||Unconformably overlies the Noonkanbah Formation. Overlain by the Alexander Formation.||
1088|Barbwire Sandstone|69312|5|Briefly described|p3, p26 fig 32|Barremian|Berriasian|Canning Basin. ||||Unconformably (or disconformably) overlies the Jarlemai Siltstone. Overlain by the Samuel Formation.|Sandstone.|
1088|Barbwire Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Oxfordian|Middle Jurassic||157-174 Ma||||Sandstone, lesser conglomerate; minor siltstone|
1088|Barbwire Sandstone|70774|5|Briefly described|p4|Late Jurassic|Middle Jurassic|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Overlain by the Alexander Formation. Equivalent to the Wallal Sandstone.||10-FEB-20
1088|Barbwire Sandstone|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Canning Basin.||||||
1088|Barbwire Sandstone|71267|4|Described|GEOL_LUT_CSV files|Oxfordian|Middle Jurassic|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|174.1-157.3 Ma (inferred)||||Prominently cross bedded and poorly sorted fine to coarse grained sandstone, intraformational conglomerate, shale, calcareous siltstone with poorly preserved plant remains.|
1088|Barbwire Sandstone|71894|5|Briefly described|p4|Upper Jurassic|Upper Jurassic|Canning Basin.||||Unconformably overlies the Erskine Sandstone. Overlain by the Alexander Formation.|Sandstone.|
1088|Barbwire Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Oxfordian|Middle Jurassic|Canning Basin. Age inferred.|||||Sandstone, lesser conglomerate; minor siltstone.|
1088|Barbwire Sandstone|72497|5|Briefly described|p3 Fig.2.|Tithonian|Callovian|Shown, along with Meda Sandstone, as  occuring in part of the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in part of the Fitzroy Trough, Betty and Balgo Terraces.||||Laterally equivalent to Jarlemai Siltstone, Alexander Formation and Wallal Sandstone. Unconformably overlain by Broome Sandstone.||
1088|Barbwire Sandstone|72499|5|Briefly described|p7 Fig.6.|Late Jurassic|Middle Jurassic|Located in the Fitzroy Trough.||||Shown as unconformably overlying Blina Shale, Erskine Sandstone and underlies Alexander Formation. Laterally equivalent to Wallal Sandstone.||
1088|Barbwire Sandstone|73117|5|Briefly described|p3|Middle Jurassic|Middle Jurassic|Canning Basin. Lower boundary marked by a major unconformity [related to the Fitzroy Transpression?].||||Overlain by Alexander Formation. Equivalent to Wallal Sandstone.|Dominantly sandstone.|
1149|Barrabiddy Member|37294|6|Mentioned|p103|||||||||
1176|Barren Sandstone|24549|6|Mentioned|p9 (table)|||Probably intended as a descriptive term for sandstone?||||||
1176|Barren Sandstone|41172|4|Described|p126|||||||||
1180|Barret Well Gneiss|40308|6|Mentioned|Table 2|||||||||
1209|Barrow Group|6876|6|Mentioned|p100 Fig.5, pp102-103|Early Cretaceous|Early Cretaceous|Seismic line shows wedge-shaped geometry resulting from delta progradation and lobe switching, and variable lithologies produce differential compaction.||||||
1209|Barrow Group|12471|6|Mentioned|p475 Fig.2, p476|Early Cretaceous|Early Cretaceous|Described as coeval with Yarraloola Conglomerate and Nannutarra Formation. A significant hydrocarbon reservoir in the Tubridgi Field.||||||27-OCT-14
1209|Barrow Group|12491|5|Briefly described|p447-448, p450-456, p459-462, p464-469..|Early Cretaceous|Late Jurassic|Barrow Sub-basin, Northern Carnarvon Basin. Thick deltaic sequences. Late Tithonian to Berriasian. Basal sandstones are reservoirs for Macedon/Pyrenees fields hydrocarbons.||||Overlies Dupuy Formation. Is overlain by Zeepaard and Birdrong Formations and Muderong Shale.||06-NOV-14
1209|Barrow Group|12525|6|Mentioned|pp45-46.|Cretaceous|Cretaceous|Exmouth Plateau. Contains Berriasian-Valanginian bentonites (ash-falls) related to a Jurassic-Cretaceous break-up event.||||||
1209|Barrow Group|13353|6|Mentioned|p412.|||Dampier Sub-basin. Well-documented hydrocarbon source potential.||||||
1209|Barrow Group|13615|4|Described|p1, p6-p8, p16, p18,|Early Cretaceous|Late Jurassic|Peedamullah Shelf, Barrow Sub-basin. Deltaic sediments. See also p27, p29, p32, p35, p38, p43, p48-p49, p51, p57, p81, p85, p88, p102 App. 3,  Plates , 2, 3.|||Includes the Flacourt Formation, Nannutarra Formation and the Yarraloola Conglomerate.|Unconformably overlain by the Winning Group.||21-JAN-22
1209|Barrow Group|14227|5|Briefly described|p11|||Geological Province: Exmouth and Barrow Sub-basins. Very thick delta deposits.||||||07-FEB-11
1209|Barrow Group|22703|4|Described|p115,118-9,124-6|Valanginian|Berriasian|Fig.3||||||
1209|Barrow Group|23355|5|Briefly described|8 Fig.1|Early Cretaceous|Early Cretaceous|||||||
1209|Barrow Group|23359|5|Briefly described|79 Tab.2|||||||||
1209|Barrow Group|23379|4|Described|p160 Fig.2;p159-164|Valanginian|Berriasian|Of Barrow Sub-basin, Carnarvon Basin.||||||10-APR-08
1209|Barrow Group|23726|5|Briefly described|p69|Valanginian|Berriasian|Geological Province: Carnarvon Basin.||||||
1209|Barrow Group|24059|4|Described|p132|Neocomian|Neocomian|Geological Province: Barrow Sub-basin. Maximum thickness: 1240m.||||||16-SEP-14
1209|Barrow Group|24084|5|Briefly described|p146 Fig.2|Early Cretaceous|Early Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
1209|Barrow Group|24085|5|Briefly described|p33, p43 Tb.2|Berriasian|Berriasian|Fluviatile-delatic deposits. Geological Province: Carnarvon Basin.||||||16-MAR-05
1209|Barrow Group|24205|5|Briefly described|p242|Early Cretaceous|Early Cretaceous|See also p250 Figs. 6 and 7.  Geological Province: Northern Carnarvon Basin.||||||
1209|Barrow Group|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
1209|Barrow Group|24315|5|Briefly described|p43|Early Cretaceous|Early Cretaceous|Overlies the Dupuy Sandstone. Unconformably underlies the Mardie Greensand Member. Geological Province: Barrow Sub-Basin.||||||09-MAR-05
1209|Barrow Group|24331|5|Briefly described|p475 Fig.2|Early Cretaceous|Early Cretaceous|Conformably overlies Dupuy Formation. Unconformably overlain by Mardie Greensand Member. Marine to fluvial. Geological Province: Barrow Sub-basin.||||||
1209|Barrow Group|24351|5|Briefly described|p24, p39|Cretaceous|Cretaceous|Massive and interbedded sands included. Geological Province: Exmouth Sub-basin.||||||13-DEC-07
1209|Barrow Group|24390|5|Briefly described|p21|Early Cretaceous|Early Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
1209|Barrow Group|24409|5|Briefly described|p49|Berriasian|Berriasian|Geological Province: Carnarvon Basin||||||
1209|Barrow Group|29721|6|Mentioned|Table 102|||||||||
1209|Barrow Group|30304|4|Described|p51|||||||||
1209|Barrow Group|30365|6|Mentioned|Fig.8|||||||||
1209|Barrow Group|31083|6|Mentioned|Fig. 4|||||||||
1209|Barrow Group|31561|4|Described|p38|||See also P34. Early Cretaceous. "Deltaic".||||||
1209|Barrow Group|31604|6|Mentioned|p6|||See also Table 4. Tithonian to Neocomian.||||||10-APR-08
1209|Barrow Group|31897|6|Mentioned|p84|||Hydrocarbon pay in Angel no.1||||||
1209|Barrow Group|32024|6|Mentioned|p18|||Jurassic.||||||
1209|Barrow Group|32025|6|Mentioned|p989|||Angel No.1 net hydrocarbon pay.||||||10-APR-08
1209|Barrow Group|32711|6|Mentioned|p446|||Fig.3||||||
1209|Barrow Group|32714|6|Mentioned|Fig.7|||||||||
1209|Barrow Group|32715|6|Mentioned|p1177|||||||||
1209|Barrow Group|33386|6|Mentioned|Fig.7|||||||||
1209|Barrow Group|33453|6|Mentioned|p71|||Depositional environment||||||
1209|Barrow Group|33813|6|Mentioned|p5|||Table 2 & Figs 5 & 6||||||
1209|Barrow Group|34363|6|Mentioned|p56|||Jurassic - Cretaceous. See Fig.7.||||||
1209|Barrow Group|34840|6|Mentioned|p66|||||||||
1209|Barrow Group|34846|6|Mentioned|Fig.3|||||||||
1209|Barrow Group|35105|6|Mentioned|Fig.5|||||||||
1209|Barrow Group|35282|6|Mentioned|Fig.21|||||||||
1209|Barrow Group|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
1209|Barrow Group|37360|6|Mentioned|Fig.3|||||||||
1209|Barrow Group|37688|6|Mentioned|p18|||||||||
1209|Barrow Group|37689|6|Mentioned|p25|||On schematic section.||||||
1209|Barrow Group|38732|6|Mentioned|p32|||||||||
1209|Barrow Group|39486|6|Mentioned|p2092|||See also P2093||||||
1209|Barrow Group|39757|6|Mentioned|p1605|||||||||
1209|Barrow Group|40617|5|Briefly described|p13|||||||||
1209|Barrow Group|40992|6|Mentioned|p13|||||||||
1209|Barrow Group|41123|6|Mentioned|p180|||||||||
1209|Barrow Group|41170|5|Briefly described|p155|||||||||
1209|Barrow Group|41271|3|Fully described|p135|||||||||
1209|Barrow Group|41365|6|Mentioned|p3|||||||||
1209|Barrow Group|41436|6|Mentioned|p46|||See also P47||||||
1209|Barrow Group|41438|4|Described|p108|||||||||
1209|Barrow Group|41439|4|Described|p122|||Informally named as Flag Sandstone.||||||01-SEP-08
1209|Barrow Group|41440|4|Described|p137|||||||||
1209|Barrow Group|41443|6|Mentioned|p158|||||||||
1209|Barrow Group|41444|4|Described|p182|||||||||
1209|Barrow Group|41445|4|Described|p189|||||||||
1209|Barrow Group|41447|4|Described|p227|||||||||
1209|Barrow Group|41454|6|Mentioned|p59|||||||||
1209|Barrow Group|41589|6|Mentioned|p118|||||||||
1209|Barrow Group|41709|6|Mentioned|p212|||||||||
1209|Barrow Group|41712|6|Mentioned|p279|||||||||
1209|Barrow Group|41732|6|Mentioned|p534|||||||||
1209|Barrow Group|42075|5|Briefly described|Fig.4 P245|||||||||
1209|Barrow Group|42116|5|Briefly described|Fig.1 P6|||||||||
1209|Barrow Group|42395|6|Mentioned|p80|||||||||
1209|Barrow Group|42463|6|Mentioned|Fig.2 P169|||||||||
1209|Barrow Group|42598|4|Described|p91|||||||||
1209|Barrow Group|42615|6|Mentioned|p35|||||||||
1209|Barrow Group|42673|6|Mentioned|p194|||||||||
1209|Barrow Group|43710|6|Mentioned|p31|||||||||
1209|Barrow Group|43711|6|Mentioned|p18|||||||||
1209|Barrow Group|43712|5|Briefly described|p11||Neocomian|||||||
1209|Barrow Group|43722|5|Briefly described|p10||Neocomian|||||||
1209|Barrow Group|43724|5|Briefly described|p29||Neocomian|||||||
1209|Barrow Group|43824|6|Mentioned|p131|||||||||
1209|Barrow Group|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||
1209|Barrow Group|43827|5|Briefly described|p193||Cretaceous|Found at ODP sites 762,763||||||
1209|Barrow Group|45142|6|Mentioned|Fig.4|||||||||
1209|Barrow Group|46808|6|Mentioned|Table 2|||||||||
1209|Barrow Group|46950|6|Mentioned|Fig.15|||||||||
1209|Barrow Group|50025|5|Briefly described|p12|Early Cretaceous|Early Cretaceous|Geological Province: Exmouth and Barrow Sub-basins.||||||18-NOV-04
1209|Barrow Group|50085|5|Briefly described|p23 Fig. 12|Early Cretaceous|Jurassic|Geological Province: Northern Carnarvon Basin.||||||
1209|Barrow Group|60118|5|Briefly described|p29|||Geological Province: Barrow Sub-basin, North Carnarvon Basin.||||||
1209|Barrow Group|60384|6|Mentioned|p243 Fig 2b|Early Cretaceous|Late Jurassic|Northern Carnarvon Basin.||||||
1209|Barrow Group|60386|6|Mentioned|p302|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin. Non-marine, deltaic-nearshore-shelf.||||||
1209|Barrow Group|60725|6|Mentioned|p35 Fig.5, p36 Fig.6, |Cretaceous|Cretaceous|||||||
1209|Barrow Group|61023|5|Briefly described|p27 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin. See also p29.||||||10-APR-08
1209|Barrow Group|61554|6|Mentioned|p625 Fig.2|||Barrow Island.||||Is overlain by Muderong Shale.||
1209|Barrow Group|61555|5|Briefly described|p237, 241, 236|Hauterivian|Tithonian|Exmouth Sub-basin. Contains multi-cycle hydrocarbon reservoir elements.|||Includes Macedon, Muiron and Pyrenees Members.|Overlies Dupuy Formation. Overlain by Muderong Formation and Gearle Siltstone.|Clastic sediments.|20-MAR-12
1209|Barrow Group|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||10-APR-08
1209|Barrow Group|62837|5|Briefly described|Table A|||Geological Province: Barrow Sub-basin.||||||01-MAR-10
1209|Barrow Group|63950|5|Briefly described|p336 Fig. 4, p334|Early Cretaceous|Early Cretaceous|Includes the Flag Sandstone. Overlies Dingo Claystone. Geological Province: northern Carnarvon Basin.||||||27-MAY-08
1209|Barrow Group|64973|5|Briefly described|p504, p504 Fig. 2, p505 Fig. 3|Valanginian|Cretaceous|Overlain unconformably by Birdrong Sandstone. Geological Province: Carnarvon Basin.||||||21-JUL-09
1209|Barrow Group|64977|5|Briefly described|p491.|Early Cretaceous|Early Cretaceous|||||Overlies Dupuy Formation. Is unconformably overlain by Mardie Greensand Member of Muderong Shale.|Sandstones.|
1209|Barrow Group|65708|5|Briefly described|p99, 104, 107|Early Cretaceous|Early Cretaceous|North West Shelf. Accommodation provided by Neocomian thermal subsidence after Greater India and Australia break-up. An important reservoir; supplied by Jurassic-Triassic source rocks (Locker Formation and Dingo Claystone).|||||Economically important fluvial-deltaic to marginal marine sandstone reservoirs.|29-JUN-22
1209|Barrow Group|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||Is overlain unconformably by Mardie Greensand.||
1209|Barrow Group|67200|5|Briefly described|p8 fig 6, p65|Cretaceous|Cretaceous||||Includes Flacourt Formation, Malouet Formation, Flag Sandstone||Interbedded sandstone and siltstone.|
1209|Barrow Group|67970|5|Briefly described|p3, pp6-10, pp13-14, p25 Fig.4.|Valanginian|Tithonian|A major deltaic sediment lobe of basin floor fans and turbidites across the southern Exmouth Plateau. Good quality gas reservoir; eg Scarborough gas field. Equivalent to the distal Forestier Claystone. Thickness c.1750 m. Scarborough 1 (1979) well found a 59 m gas column in the lower part of this unit; subsequent wells extended the size of the field.|||||Sandstone, siltstone and claystone.|
1209|Barrow Group|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||||Unconformably overlies Dupuy and Angel Formations.||14-SEP-17
1209|Barrow Group|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13, Ch3 p23|||Carnarvon Basin. See also  Ch3 p35, Ch3 p65-p66, Ch3 p73. ||||||
1209|Barrow Group|69692|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Northern Carnarvon Basin.||||Overlies Dingo Formation. Is overlain by Muderong Formation and Mardie Greensand.||
1209|Barrow Group|70066|5|Briefly described|Exmouth: Fig.2; p1-3. Regional: Fig.6|Valanginian|Tithonian|See also Regional: p6, p8-10, p12. Northern Carnarvon Basin. Up to 2500m thick. Sandstone units with intra-formational claystone seals are potential reservoirs. Hosts the giant Scarborough gas accumulation.||||Overlies Dingo Claystone or Angel Formation. Is overlain by Flag Sandstone, Zeepaard Formation or Winning Group.|Basin-floor fan sandstones, pro-delta to foreset claystones, and top-set sandstones. Sandstones are predominantly quartzose, weakly cemented, with excellent porosity and permeability.|
1209|Barrow Group|70906|5|Briefly described|p757-758, p764|Early Cretaceous|Early Cretaceous|Gorgon Platform. Polygonal fault system described.||||Overlies Dingo Claystone. Is overlain by Muderong Shale.||
1209|Barrow Group|73564|5|Briefly described|p1223, 1225-1226, 1228-1232, 1236-1237|Cretaceous|Cretaceous|Exmouth Plateau, Gascoyne Margin. A c.3.5km thick rift sequence. Possibly sourced from uplift and erosion of the onshore South Carnarvon Basin to the south.||||Overlies Dingo Claystone. Is overlain by Zeepaard Formation.|Clastic deltaic rocks.|
1209|Barrow Group|73574|6|Mentioned|p762-763|Valanginian|Tithonian|North Carnarvon Basin. Early Valanginian minimum age.||||Possible offshore correlative of Yarraloola Conglomerate||
1240|Bassett Formation|7142|6|Mentioned|p350 Fig.4.|Paleogene|Late Cretaceous|Browse Basin.||||Overlies Puffin Formation. Is overlain by Prion and Grebe Formations.||
1240|Bassett Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|||||Overlies Puffin Formation. Is overlain by Prion and Grebe Formations.||
1240|Bassett Formation|13354|6|Mentioned|p375 Fig.6.|Palaeogene|Palaeogene|Unit of Woodbine Group. Overlies Puffin Formation of Bathurst Island Group and underlies Grebe and Prion Formations.||116||||28-OCT-14
1240|Bassett Formation|42053|5|Briefly described|Fig.3 p30|||||||||30-APR-12
1240|Bassett Formation|63358|5|Briefly described|p4 Fig. 1.3|Paleocene|Maastrichtian|||||||
1240|Bassett Formation|69297|5|Briefly described|p305|Ypresian|Danian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlies the Puffin Formation.||
1240|Bassett Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Ypresian|Danian|See also Northern: Fig.2; p1, p3. Yampi: Fig.2. Browse Basin. Oil show in the Phrixus 1 well. Potential intraformational seals.||Woodbine Group.||Overlies Puffin Formation. Equivalent to Johnson Formation.||12-JUL-16
1242|Bastion Group|22716|5|Briefly described|table4, p236|Mesoproterozoic|Mesoproterozoic|May be equivalent to part of the Birrindudu Group.||||||
1242|Bastion Group|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone and mudstone.   Age: c.1500Ma.  Geological Province: Bastion Basin.||||||
1242|Bastion Group|29380|6|Mentioned|p8|||||||||
1242|Bastion Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
1242|Bastion Group|30892|4|Described|p249|||Carpentarian age||||||
1242|Bastion Group|30894|4|Described|p249|||Carpentarian age.||||||
1242|Bastion Group|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1242|Bastion Group|31393|6|Mentioned|Pl.25|||||||||
1242|Bastion Group|31662|6|Mentioned|Fig. 1|||||||||
1242|Bastion Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1242|Bastion Group|32660|4|Described|Table 3|||||||||
1242|Bastion Group|32663|6|Mentioned|p10|||||||||
1242|Bastion Group|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
1242|Bastion Group|32728|6|Mentioned|Fig.3|||||||||
1242|Bastion Group|34137|4|Described|Table 1||Carpentarian|Includes Mendena Formation, (SD52-13). Carpentarian.||||||
1242|Bastion Group|34462|4|Described|Table 1|||Carpentarian. See P9||||||
1242|Bastion Group|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1242|Bastion Group|36003|6|Mentioned|p1028|||||||||
1242|Bastion Group|36551|6|Mentioned|Table 10|||||||||
1242|Bastion Group|36885|4|Described|p183|||||||||
1242|Bastion Group|37462|4|Described|Table4.III|||||||||
1242|Bastion Group|38988|6|Mentioned|Fig.4|||||||||
1242|Bastion Group|41987|6|Mentioned|p73|||||||||
1242|Bastion Group|43595|5|Briefly described|p443|||||||||
1242|Bastion Group|43652|6|Mentioned|p385|||||||||
1242|Bastion Group|44140|4|Described|p293-294, p296 fig 4-3, p299|Paleoproterozoic|Paleoproterozoic|Up to 1400 m thick in north of Kimberley Basin.|>1762 +/- 15 Ma.||Mendena Formation, Wyndham Shale, Cockburn Sandstone.|Overlies Kimberley Group conformably.|Purple and green shale, siltstone and small amounts of sandstone and dolomite, topped by massive quartz sandstone.|07-MAR-18
1242|Bastion Group|44155|6|Mentioned|p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|Kimberley region.||||||
1242|Bastion Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
1242|Bastion Group|44286|5|Briefly described|Map legend|||||||||
1242|Bastion Group|44363|4|Described|p.19|||(Carpentarian) units.||||||
1242|Bastion Group|44364|14|Not recorded|map legend|||||||||
1242|Bastion Group|44366|14|Not recorded|p.16, Table 2||Carpentarian|||||||
1242|Bastion Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
1242|Bastion Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1242|Bastion Group|45047|5|Briefly described|p28|||Carpentarian.||||||
1242|Bastion Group|48931|6|Mentioned|p45|||Stratigraphy||||||
1242|Bastion Group|61861|5|Briefly described|Fig.2, p23|||Halls Creek, eastern zone. Correlated with Birrindudu Group of Tanami Region.||||Unconformably overlies Kimberley Group.||
1242|Bastion Group|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|[This article changes the age of a number of units, including this one, without explanation. Error in Figure 10?]||||||19-MAY-15
1242|Bastion Group|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Sandstone, siltstone, and mudstone.||||||18-MAY-15
1242|Bastion Group|64724|6|Mentioned|p45 Fig.5|Calymmian|Calymmian|Kimberley Basin||||||
1242|Bastion Group|64748|4|Described|p268, p275|Statherian|Orosirian|Unconformably overlies the Kimberley Group in the north east; includes the Wyndham Shale; correlated with the Birrindudu Group; underlies the Carr Boyd Group||||||
1242|Bastion Group|67563|6|Mentioned|p121|||Kimberley Basin.||||||
1242|Bastion Group|68992|6|Mentioned|p499|||Kimberley Basin.||||||
1242|Bastion Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
1242|Bastion Group|69099|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic||||||sandstone, siltstone, and mudstone|18-MAY-15
1242|Bastion Group|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Mesoproterozoic||||||undivided; sandstone, siltstone and mudstone.|
1242|Bastion Group|69585|6|Mentioned|p17|Paleoproterozoic|Paleoproterozoic|||||Unconformably overlies Pentecost Sandstone.||
1242|Bastion Group|69587|6|Mentioned|2_5m_geologyp98_lut.csv|||||||||
1242|Bastion Group|69597|6|Mentioned|p5 fig 2b|||||||||
1242|Bastion Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Mesoproterozoic||||||Undivided; sandstone, siltstone, and mudstone|
1242|Bastion Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Misspelt as the Baston Group in 2_5m_geologyp98_lut.csv. |1640-1797 Ma||||Sandstone, siltstone and mudstone.|
1242|Bastion Group|70731|5|Briefly described|p268,270,278|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.|<1797 Ma|||Underlain by Kimberley Group.||
1242|Bastion Group|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Bastion Basin.||||||
1242|Bastion Group|70851|5|Briefly described|p6, p17-p18, p29|||||||Overlies the Kimberley Group, Upper. Overlain by the Carr Boyd Group and the Duerdin Group.||
1242|Bastion Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Bastion Basin. Events: North Australian Craton events (2500-250 Ma). See 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1797-1640 Ma (inferred)||Includes Cockburn Sandstone, Mendena Formation, Wyndham Shale.||Sandstone, siltstone, and mudstone|
1242|Bastion Group|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Bastion Basin, North Australian Craton.|||Mendena Formation.|||
1242|Bastion Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Bastion Basin.|||||Sandstone, siltstone, and mudstone.|
1242|Bastion Group|73255|6|Mentioned|p533 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
1249|Bathurst Island Group|5952|6|Mentioned|p222|||||||||
1249|Bathurst Island Group|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cretaceous|Cretaceous|2km thick. Absent south of 14oS.||Bathurst Island Group||Overlies Flamingo Group, Sahul Group, Troughton Group, Ashmore Volcanics.||
1249|Bathurst Island Group|13224|5|Briefly described|p485 fig 3, p487,  p488|Maastrichtian|Valanginian|||||||
1249|Bathurst Island Group|13234|5|Briefly described|p250 Fig.2, p252 Fig.4, p263 Tb.4, |Cretaceous|Cretaceous|Basal sands are a potential reservoir. Intraformational marls and shales are a potential regional seal.||||Overlies Flamingo Group.||
1249|Bathurst Island Group|13354|6|Mentioned|p375 Fig.6.|Cretaceous|Cretaceous|Comprises, in ascending order, Echuca Shoals, Jamieson, Woolaston, Gibson, Fenelon and Puffin Formations. Overlies Swan Group and underlies Woodbine Group.||155||||28-OCT-14
1249|Bathurst Island Group|23183|6|Mentioned|p218|Cenomanian||||||||26-JUL-06
1249|Bathurst Island Group|23377|6|Mentioned|p212 Fig.5||Cretaceous|of Vulcan Sub-basin.||||||
1249|Bathurst Island Group|23378|4|Described|p180 Fig.2|Late Cretaceous|Early Cretaceous|Of Vulcan Sub-basin.||||||01-MAR-10
1249|Bathurst Island Group|23937|6|Mentioned|p55|Cretaceous|Cretaceous|||||||
1249|Bathurst Island Group|23999|5|Briefly described|p8|Cenomanian|Aptian|Formerly the Bathurst Island Formation. Age range: 112-93Ma.||||||07-FEB-11
1249|Bathurst Island Group|24047|5|Briefly described|p13|Cretaceous|Cretaceous|Includes the Wangarlu Formation and Moonkinu Sandstone.  Geological Province: Money Shoal Basin.||||||
1249|Bathurst Island Group|24085|5|Briefly described|p34|Cretaceous|Cretaceous|Includes Darwin Formation, Marligar Formation, Wangarlu Mudstone and Moonkinu Formation.||||||20-JUL-06
1249|Bathurst Island Group|24122|5|Briefly described|p14|Cretaceous|Cretaceous|Includes the Darwin Formation.||||||
1249|Bathurst Island Group|24297|5|Briefly described|p21|Cretaceous|Cretaceous|||||||
1249|Bathurst Island Group|24569|5|Briefly described|p248 Fig. 3|Late Cretaceous|Early Cretaceous|Includes the Wangarlu and Darwin Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
1249|Bathurst Island Group|41459|6|Mentioned|Fig.2|||||||||
1249|Bathurst Island Group|41532|3|Fully described|p306|||||||||
1249|Bathurst Island Group|41690|5|Briefly described|p6|||See also p73 and p109||||||20-JUL-06
1249|Bathurst Island Group|41731|6|Mentioned|Fig.3|||||||||
1249|Bathurst Island Group|41733|6|Mentioned|p547|||||||||
1249|Bathurst Island Group|42003|5|Briefly described|p143|||||||||
1249|Bathurst Island Group|42034|4|Described|Fig.4 P11|||||||||
1249|Bathurst Island Group|42053|5|Briefly described|Fig.17 P47|||||||||01-MAR-10
1249|Bathurst Island Group|42058|5|Briefly described|Fig.10 P114|||||||||
1249|Bathurst Island Group|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
1249|Bathurst Island Group|42442|3|Fully described|p27|||||||||
1249|Bathurst Island Group|42861|5|Briefly described|p3|||||||||
1249|Bathurst Island Group|43661|6|Mentioned|Fig.3|||||||||
1249|Bathurst Island Group|43699|6|Mentioned|p3||Cretaceous|||||||
1249|Bathurst Island Group|43707|5|Briefly described|Fig.3,p4-5||Cretaceous|||||||
1249|Bathurst Island Group|43739|6|Mentioned|p10||Cretaceous|||||||
1249|Bathurst Island Group|49637|5|Briefly described|p7|Cretaceous|Cretaceous|Thickness: up to 1200m. Potential for gas and oil generation. See also Fig. 3 and 6.||||||07-FEB-11
1249|Bathurst Island Group|60386|6|Mentioned|p302|Aptian|Valanginian|Bonaparte Basin. Distal shelf/basin. ||||||
1249|Bathurst Island Group|60634|6|Mentioned|p1167 Fig.2,  p1168 Fig.3.||||||Includes Echuca Shoals, Jamieson, Woolaston, Gibson, Fenelon, Borde and Puffin Formations.|Overlies Swan Group. Is overlain by Woodbine Group.||
1249|Bathurst Island Group|60677|6|Mentioned|Map Legend|Cretaceous|Cretaceous|||||||11-JAN-05
1249|Bathurst Island Group|61550|6|Mentioned|p495 Fig.2. |Maastrichtian|Berriasian||||Includes the Puffin, Fenelon, Gibson, Woolaston, Jamieson and Echuca Shoals Formation.|Overlies Swan Group. Is overlain by Woodbine Group.||
1249|Bathurst Island Group|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Jurassic|Includes Darwin, Echuca Shoals, Jamieson, Woolaston, Gibson, Fenelon, Puffin and Wangarlu Formations. Age: ~137-70Ma. Geological Province: Londonderry High.||||||01-MAR-10
1249|Bathurst Island Group|63062|5|Briefly described|p9 Fig. 9, p35|Maastrichtian|Aptian|Also shown as Upper and Lower Bathurst Isalnd Group. Geological Province: Arafura and Money Shoal Basins. Deltaic and open marine deposits. See also p32 Fig. 29||||||07-FEB-11
1249|Bathurst Island Group|63358|5|Briefly described|p172 Ap. Table A1.11|||||||||01-MAR-10
1249|Bathurst Island Group|65339|6|Mentioned|p6 Table 1, p16.||||||Includes Darwin Formation.|||
1249|Bathurst Island Group|66187|5|Briefly described|p413 Fig.2|Maastrichtian|Valanginian|Mount Ashmore Dome, Bonaparte Basin. Includes Puffin, Fenelon, Gibson, Woolaston, Jamieson and Echuca Shoals Formations.||||||
1249|Bathurst Island Group|67564|6|Mentioned|p51.|Late Aptian|Late Aptian|Southern shelf succession of the Money Shoal Basin. Marine sedimentary rocks.||||||
1249|Bathurst Island Group|69297|5|Briefly described|p283,  p285, p305, p322|Maastrichtian|Aptian |Money Shoal Basin and Barcoo, Seringapatam and Caswell Sub-basins of the Browse Basin. Deposited in marine or deltaic environments across a shallow marine shelf.  |||Includes the Echuca Shoals Formation, the Lower and Upper Jamieson Formations and the Woolaston, Gibson, Fenelon and Puffin Formations.|Overlies the Swan Group. Unconformably overlain by the Woodbine Group.|Mudstones and marls with interbedded sandstones.|
1249|Bathurst Island Group|69418|6|Mentioned|p3:28|||Money Shoal Basin. Hosts the Araru Point, Croker Island and Vashon Head residual bauxite deposits (described).||||||12-JUL-16
1249|Bathurst Island Group|69420|6|Mentioned|p5:118||||||Darwin Formation.|||12-JUL-16
1249|Bathurst Island Group|69451|6|Mentioned|p35:2 Fig.35.2; 35:3 Fig.35.4; 35:14|Cretaceous|Cretaceous|Money Shoal Basin. Could provide a regional seal for underlying Paleozoic rocks of the Arafura Basin.||||||12-JUL-16
1249|Bathurst Island Group|69452|4|Described|p36:4-5, 7-8, 15, 22|Cretaceous|Cretaceous|Mory (1988); originally the Bathurst Island Formation of Hughes and Senior (1974); Hughes (1978). Bonaparte Basin and into Browse Basin. Referred to as "Bathurst Island Group equivalent". Up to 2,000m thick (mostly Wangarlu Formation), thinning to the W to be 100-300m thick on the Ashmore Platform.|||Echuca Shoals, Darwin, Wangarlu, Jamieson, Brown Gannet, Woolaston, Gibson, Fenelon, Turnstone Formations.|Is overlain unconformably by Woodbine Group.|Thick, shale-dominated marine sedimentary rocks.|12-JUL-16
1249|Bathurst Island Group|69456|3|Fully described|p40:1-9, 12, 15|Late Cretaceous|Early Cretaceous|Mory (1988). Originally defined as Bathurst Island Formation (Hughes and Senior, 1984; Hughes, 1978). Money Shoal, Bonaparte and Browse Basins. Mainly located offshore (2km thick) but occurs onshore in northern NT (83m thick in Gunn Point-1). Deltaic to open marine environments, deepening to the W. The base of the Group is diachronous, younging to the E (Valanginian-Maastrichtian). Hosts lateritic bauxite in the Cobourg Peninsula-Croker Island area. Fair to good petroleum source potential; mudstones could provide a regional seal.|||Darwin, Marligur and Wangarlu Formations; Moonkinu Sandstone.|Unconformably overlies Plover Formation or Flamingo Group. Is overlain unconformably by Woodbine Group and Van Diemen Sandstone.|Mostly fine-grained rocks including claystone, marl and siltstone with locally thick interbeds of mostly fine-grained sandstone.|12-JUL-16
1249|Bathurst Island Group|69653|5|Briefly described|p1, 6, 8, 13 Fig.2.4, p15, 18, 34, 36-37|Cretaceous|Cretaceous|Petrel Sub-basin.  Widespread marine transgression deposits.  Suitable as a regional seal for CO2 storage in Sandpiper Sandstone. Photomicrographs. See also p53-55, 60-61, 70, 73-76.|||Darwin, Echuca, Wangarlu Formations.|Overlies Flamingo Group. Is overlain by Woodbine Group.|Fine-grained clastic and carbonate sediments.|
1249|Bathurst Island Group|69673|6|Mentioned|p166 fig 136, p173, p204, p205|Cretaceous|Cretaceous||||Includes Darwin Formation, Marligur Formation, Wangarlu Formation, Moonkinu Sandstone|||
1249|Bathurst Island Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2, p3|Maastrichtian|Valanginian|See also Regional geology: Figs.6-7, p6, p11-12, p14. Sahul: Fig.2, p1-3. Vulcan: Fig.2. Marine shales form a regional seal, although polygonal faulting "needs further investigation". Contains high-quality reservoirs, eg Darwin and Woolaston Formations.|||Echuca Shoals, Darwin, Wangarlu, Jamieson, Woolaston, Fenelon and Turnstone Formations; Brown Gannet Limestone.|Overlies Flamingo Group. Is overlain by Woodbine Group.|Fine-grained clastics and carbonates.|12-JUL-16
1249|Bathurst Island Group|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Maastrichtian|Valanginian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.|||Echuca Shoals, Lower and Upper Jamieson, Lower and Upper Heywood, Woolaston, Fenelon and Puffin Formations; Brown Gannet Limestone.|Overlies Swan Group. Is overlain by Woodbine Group.||12-JUL-16
1249|Bathurst Island Group|70098|5|Briefly described|p18 Fig.4, p19 Fig.5|Cretaceous|Cretaceous|Shown as Upper Bathurst Island Group and Lower Bathurst Island Group in Fig.4.||||Overlies Flamingo Group. Is overlain by Woodbine Group.||28-SEP-16
1249|Bathurst Island Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
1249|Bathurst Island Group|73083|6|Mentioned|p17, p33|Cretaceous|Cretaceous|Money Shoal Basin.||||||
1314|Beaconsfield Conglomerate|36293|2|Defined|p56|Proterozoic|Proterozoic|||||||
1314|Beaconsfield Conglomerate|36872|3|Fully described|p73|||||||||
1314|Beaconsfield Conglomerate|37460|6|Mentioned|p178|||||||||
1314|Beaconsfield Conglomerate|40307|6|Mentioned|Fig.2|||||||||
1314|Beaconsfield Conglomerate|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1314|Beaconsfield Conglomerate|40347|6|Mentioned|p16|||||||||
1314|Beaconsfield Conglomerate|42441|5|Briefly described|p77|||Proterozoic||||||
1314|Beaconsfield Conglomerate|43495|6|Mentioned|5|||||||||
1348|Beckett Member|15881|5|Briefly described|p62|Permian|Permian|Of Holmwood Shale in the Irwin and Lockier River valley areas. Contains ammonoids.||||||12-FEB-09
1348|Beckett Member|22820|5|Briefly described|p10 Fig.4|Early Permian|Early Permian|Of Holmwood Shale.||||||11-AUG-08
1348|Beckett Member|23172|4|Described|Map Legend|Permian|Permian|||||||
1348|Beckett Member|23174|5|Briefly described|Fig5p8,10|Early Permian|Early Permian|||||||
1348|Beckett Member|23279|6|Mentioned|p12|||Miswritten for Beckett Limestone Member.||||||
1348|Beckett Member|23816|5|Briefly described|p232|Sakmarian|Sakmarian|Geological Province: Perth Basin. Of the Holmwood Shale.||||||
1348|Beckett Member|30948|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
1348|Beckett Member|30963|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
1348|Beckett Member|30973|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
1348|Beckett Member|31037|6|Mentioned|p1035|||Ammonoid coquina||||||
1348|Beckett Member|31910|5|Briefly described|Table 1|||See P16||||||
1348|Beckett Member|32337|5|Briefly described|p24|||||||||
1348|Beckett Member|32649|4|Described|p22|||See also Table 1||||||
1348|Beckett Member|36293|6|Mentioned|p91|||||||||
1348|Beckett Member|36890|4|Described|p232|||||||||
1348|Beckett Member|37294|6|Mentioned|p104|||||||||
1348|Beckett Member|38217|5|Briefly described|p269|||||||||
1348|Beckett Member|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
1348|Beckett Member|40347|6|Mentioned|p23|||||||||
1348|Beckett Member|41315|6|Mentioned|p149|||||||||
1348|Beckett Member|41514|5|Briefly described|p62|||Of the Holmwood Shale.  Contains ammonoids.||||||18-AUG-08
1348|Beckett Member|43015|5|Briefly described|Table 1,p319|||||||||
1348|Beckett Member|43067|6|Mentioned|p119|||of Holmswood Shale||||||
1348|Beckett Member|43296|5|Briefly described|Map Legend||Permian|of Holmwood Shale||||||
1348|Beckett Member|43495|4|Described|10|Sakmarian|Asselian|||||||
1348|Beckett Member|48848|14|Not recorded|p.95|||||||||
1348|Beckett Member|49644|5|Briefly described|Table|||||||||
1348|Beckett Member|61811|5|Briefly described|p36.|Permian|Permian|Lenticular calcareous facies of restricted areal extent.||Unit in Holmwood Shale.||||
1348|Beckett Member|64635|6|Mentioned|p18-19 |Sakmarian|Sakmarian|||Unit in Holmwood Shale.|||Local, lenticular calcareous facies.|
1348|Beckett Member|64974|5|Briefly described|p144 Fig. 3|Sakmarian|Sakmarian|Of Holmwood Shale. Geological Province: Perth Basin.||||||24-JUN-09
1348|Beckett Member|69547|4|Described|p197|Sakmarian|Sakmarian|northern Perth Basin. Located in the lower section of the Holmwood Shale. Contains a monospecific assemblage of large ammonoids (Juresanites).||Unit of Holmwood Shale.||Overlain and underlain by Holmwood Shale mudstone.|Thin calcareous mudstone.|
1348|Beckett Member|73623|5|Briefly described|p3, 6|||Playford et al. (1976). Irwin Basin. Appears as Beckett Limestone Member on p3.||Holmwood Shale||Equivalent to Beckett Limestone Member.|Localised nodular limestone deposits containing unusual fossil biota including tube worms, bivalve-like shells, gastropods and ammonoids.|
1384|Beedagong Claystone|14228|6|Mentioned|p9|Cretaceous|Cretaceous|Of Shafik (1990). [Misquoted] here as 'Beedagong Shale'. Formerly included Haycock Marl, but this considered invalid since it contains some Campanian strata better placed in Toolonga Calcilutite.||||Haycock Marl synonymous.||05-OCT-16
1384|Beedagong Claystone|23355|5|Briefly described|13|||||||||
1384|Beedagong Claystone|23379|6|Mentioned|p159||Turonian|||||||
1384|Beedagong Claystone|23915|5|Briefly described|p539-540|Santonian|Turonian|Replaces: Upper Gearle Siltstone.  Max. Thickness: 83m.||||||
1384|Beedagong Claystone|24351|5|Briefly described|Plate 4 (in pocket)|Late Cretaceous|Late Cretaceous|Geological Province: Exmouth Sub-basin and Gascoyne Platform/Sub-basin.||||||13-DEC-07
1384|Beedagong Claystone|42123|4|Described|p31|||Reserved as Beedagong Formation See also Fig.7||||||
1384|Beedagong Claystone|42995|2|Defined|p31||Cretaceous|see also Table 1.  Middle Cretaceous||||||
1384|Beedagong Claystone|43564|6|Mentioned|Fig.2,p446|Santonian|Cenomanian|||||||
1384|Beedagong Claystone|43598|6|Mentioned|p813|||||||||
1384|Beedagong Claystone|62837|5|Briefly described|Stratigraphic columns|Turonian|Early Cretaceous|Age: 90-85Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
1384|Beedagong Claystone|70066|5|Briefly described|Regional: Fig.6|Santonian|Turonian|Exmouth and Barrow Sub-basins, Northern Carnarvon Basin.||||Overlies Gearle Siltstone. Is overlain by Toolonga Calcilutite.||23-SEP-18
1401|Bejah Claystone|7433|5|Briefly described|p25 Fig.2, p42, p47. |Albian|Aptian|Canning and Officer Basins. Marine fine clastics. Maximum thickness 14 m in Canning Basin. Contains pelecypods and radiolaria.||||Overlies Samuel Formation.|Claystone; minor siltstone; rare very fine sandstone.|
1401|Bejah Claystone|22707|5|Briefly described|p15, Table1 p7|Mesozoic|Early Cretaceous|||||||02-APR-19
1401|Bejah Claystone|23585|6|Mentioned|p25|||||||||
1401|Bejah Claystone|24067|5|Briefly described|p252|Aptian|Aptian|Geological Province: Officer Basin.||||||
1401|Bejah Claystone|31153|6|Mentioned|p111|||Re bivalves of Officer Basin||||||
1401|Bejah Claystone|31455|4|Described|Table 2|||||||||
1401|Bejah Claystone|31632|4|Described|p13|||On Table 2||||||
1401|Bejah Claystone|31633|4|Described|Table 2|||Mention P7.||||||
1401|Bejah Claystone|31639|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|31640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|31914|2|Defined|p98|Aptian|Aptian|Reference section for Officer Basin given.||||||01-SEP-14
1401|Bejah Claystone|33587|3|Fully described|p9|||Table 2.||||||
1401|Bejah Claystone|33595|6|Mentioned|p16|||||||||
1401|Bejah Claystone|33597|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|35123|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|35222|6|Mentioned|p14|||||||||
1401|Bejah Claystone|35250|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|35387|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|35902|4|Described|Table 1|||||||||
1401|Bejah Claystone|35903|4|Described|Table 1|||||||||
1401|Bejah Claystone|36257|6|Mentioned|Table 2.1|||||||||
1401|Bejah Claystone|36701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
1401|Bejah Claystone|36890|3|Fully described|p354|||Formerly Bejah Beds.||||||09-DEC-08
1401|Bejah Claystone|37916|5|Briefly described|p466|||||||||
1401|Bejah Claystone|38878|6|Mentioned|Map legend|Albian|Albian|||||||
1401|Bejah Claystone|39211|5|Briefly described|p53|||||||||
1401|Bejah Claystone|40934|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
1401|Bejah Claystone|40938|6|Mentioned|Fig.3|||||||||
1401|Bejah Claystone|41271|6|Mentioned|p152|||||||||
1401|Bejah Claystone|42442|6|Mentioned|p36|||Officer/Southern Canning Basin.||||||09-DEC-08
1401|Bejah Claystone|43595|6|Mentioned|Fig 3-43,p348||Cretaceous|||||||
1401|Bejah Claystone|44145|6|Mentioned|p553, p554|||Officer Basin rocks.||||Near basin margin, grades laterally into Toondi Formation? and to south, grades laterally into Madura Formation.||
1401|Bejah Claystone|44354|5|Briefly described|Map Legend||Early Cretaceous|||||||
1401|Bejah Claystone|45104|5|Briefly described|p30|||||||||
1401|Bejah Claystone|45149|3|Fully described|Table 1|||See also Fig.12.||||||
1401|Bejah Claystone|45153|2|Defined|App.8-141|Aptian|Aptian|Formerly Bejah beds.||||||
1401|Bejah Claystone|45158|3|Fully described|p12|||||||||
1401|Bejah Claystone|46975|6|Mentioned|p86|||||||||
1401|Bejah Claystone|61155|5|Briefly described|p16|||Age is pre-Cainozoic. Geological Province: Southern Canning Basin.||||||03-MAR-10
1401|Bejah Claystone|64580|4|Described|map legend||Early Cretaceous|Radiolarian siltstone.||||||09-DEC-08
1401|Bejah Claystone|64970|6|Mentioned|p720|||Geological Province: Officer Basin. Interbedded sandstones and claystones of marine origin.||||||27-MAY-09
1401|Bejah Claystone|65102|4|Described|p.366,369,374, Figs4-41,4-49, Table4-15|Aptian|Valanginian|Officer Basin. 3-35m; radiolarian claystone; minor siltstone & fine sandstone; marine, open shelf; conformable on Samuel Formation; disconformable on Paterson Formation; type section approx. 30km NW of Mount Beadell, 25deg 28min S, 125deg 06min E. ||||||
1401|Bejah Claystone|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||23-FEB-10
1401|Bejah Claystone|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Samuel Formation and Frezier Sandstone.||
1401|Bejah Claystone|67195|4|Described|p19 table 1, p45, 47 , App 2|||Western Officer Basin. Thermal conductivity of 1.33 W/mK|||||Salmon pink to cream claystone with frequent pink-purple mottling; very light and almost porcelaneous.|
1401|Bejah Claystone|67200|5|Briefly described|app 2 p10||||||||Mottled claystone, very light and almost porcelaneous.|
1401|Bejah Claystone|68007|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||||25-FEB-20
1401|Bejah Claystone|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Samuel Formation, Frezier Sandstone.||
1401|Bejah Claystone|69153|6|Mentioned|500k_geologyp08_lut.csv||Early Cretaceous|Lithology description shared with Samuel Formation.|||||Siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic, radiolarian siltstone|
1401|Bejah Claystone|69182|6|Mentioned|Ch4 p9, Ch4 p45,Ch4 p47|Early Cretaceous|Early Cretaceous|Canning Basin. ||||Overlies the Samuel Formation and the Frezier Sandstone.||10-FEB-20
1401|Bejah Claystone|70634|4|Described|500k_geolgyp08_lut.csv|Early Cretaceous|Early Cretaceous|Included with Samuel Formation in file (Undivided)|||||undivided; siltstone, sandstone and claystone; micaceous, carbonaceous; locally glauconitic, radiolarian siltstone in Bejah Claystone|
1401|Bejah Claystone|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Willara and Kidson Sub-basins, Canning Basin.||||Overlies the Samuel Formation and Frezier Sandstone.||10-FEB-20
1401|Bejah Claystone|70793|4|Described|500k_interpgeop14_lut.csv|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)||||Siltstone, sandstone and claystone; carbonaceous, locally glauconitic; radiolarian siltstone in Bejah Claystone|
1401|Bejah Claystone|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Gunbarrel Basin.||||||
1401|Bejah Claystone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone, radiolarite|
1401|Bejah Claystone|71268|4|Described|GEOL_LUT_CSV files|Albian|Aptian|Of Gunbarrel Basin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-southern margin (100.5-93.9 Ma); Aptian transgression (123-121 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|125-100.5 Ma (biostrat)|||Correlable with Samuel Formation.|Siltstone, sandstone and claystone; carbonaceous, locally glauconitic; radiolarian siltstone|
1401|Bejah Claystone|72034|6|Mentioned|500k_interpgeop16_lut|Albian|Aptian|Gunbarrel Basin. Shown as informal combination with Samuel Formation. Age from biostratigraphy.||||||
1401|Bejah Claystone|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Willara Sub-basin.||||Overlies Samuel Formation, Frezier Sandstone. Laterally equivalent to Anketell Formation.|Includes shale and some sandstone.|
1401|Bejah Claystone|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Samuel Formation and Frezier Sandstone. Equivalent to Anketell Formation.|Dominantly shale and mudstone with lesser sandstone.|
1401|Bejah Claystone|73346|6|Mentioned|p28|Cretaceous|Cretaceous|Ryan Shelf.||||Unconformably underlain by Grant Group.||
1411|Belcher Subgroup|41997|6|Mentioned|p79|||||||||
1447|Belvedere Group|42260|5|Briefly described|p115|||reserved as Belvedere Volcanics but tagged NLR in 1984.||||||
1491|Bentley Supergroup|23745|5|Briefly described|p15|Neoproterozoic|Mesoproterozoic|Age: 1064+/-23 Ma.||||||
1491|Bentley Supergroup|24017|5|Briefly described|p9 Tb. 2|||||||||
1491|Bentley Supergroup|24197|5|Briefly described|p97|||Includes the Tollu Group. Overlies the Giles Complex. Geological province: Musgrave Complex.||||||07-FEB-11
1491|Bentley Supergroup|24496|4|Described|p1, 15|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050 Ma. Bimodal volcanics and sediments deposited in a regional zone of transtensile shear. Unconformably overlies Birksgate Complex. Equivalent to the Tjauwata Group. Geological Province: Musgrave Block.||||||15-JUL-08
1491|Bentley Supergroup|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050Ma.  Geological Province: Musgrave Block.||||||
1491|Bentley Supergroup|24499|5|Briefly described|Map legend|||||||||
1491|Bentley Supergroup|30385|6|Mentioned|p8|||||||||
1491|Bentley Supergroup|30386|4|Described|p5|||Proterozoic age.See also p6-8||||||25-JUL-06
1491|Bentley Supergroup|30388|4|Described|Table 1|||Proterozoic age.||||||06-AUG-08
1491|Bentley Supergroup|30389|6|Mentioned|p15|||||||||
1491|Bentley Supergroup|30390|4|Described|p49|||Middle Proterozoic age||||||
1491|Bentley Supergroup|30391|6|Mentioned|p456|||||||||
1491|Bentley Supergroup|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
1491|Bentley Supergroup|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Includes Mission Group, Cassidy Group and Pussy Cat Group.||||||
1491|Bentley Supergroup|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
1491|Bentley Supergroup|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
1491|Bentley Supergroup|33468|6|Mentioned|p212|||See also p214. Equivalents||||||25-JUL-06
1491|Bentley Supergroup|33478|6|Mentioned|p451|||||||||
1491|Bentley Supergroup|34688|6|Mentioned|p341|||||||||
1491|Bentley Supergroup|35255|6|Mentioned|p7|||||||||
1491|Bentley Supergroup|35308|6|Mentioned|p451|||||||||
1491|Bentley Supergroup|35323|6|Mentioned|p404|||||||||
1491|Bentley Supergroup|35726|6|Mentioned|p102|||||||||
1491|Bentley Supergroup|36551|6|Mentioned|p22|||See also p115.||||||25-JUL-06
1491|Bentley Supergroup|36886|3|Fully described|p196|||||||||
1491|Bentley Supergroup|37299|6|Mentioned|Fig.1|||||||||
1491|Bentley Supergroup|37460|4|Described|p175|||||||||
1491|Bentley Supergroup|37707|6|Mentioned|p11|||See also p24.||||||25-JUL-06
1491|Bentley Supergroup|38157|6|Mentioned|p277|||||||||
1491|Bentley Supergroup|38243|6|Mentioned|p355|||||||||
1491|Bentley Supergroup|38988|6|Mentioned|p17|||||||||
1491|Bentley Supergroup|39120|6|Mentioned|p146|||||||||
1491|Bentley Supergroup|42940|6|Mentioned|p1|||||||||
1491|Bentley Supergroup|43052|6|Mentioned|p160|||||||||
1491|Bentley Supergroup|43118|6|Mentioned|p28|||||||||
1491|Bentley Supergroup|43348|6|Mentioned|P15|||||||||
1491|Bentley Supergroup|43595|5|Briefly described|p447|||||||||
1491|Bentley Supergroup|43693|5|Briefly described|p107|||||||||
1491|Bentley Supergroup|43695|6|Mentioned|p69|||||||||
1491|Bentley Supergroup|43696|6|Mentioned|p41|||||||||
1491|Bentley Supergroup|43697|6|Mentioned|p27|||||||||
1491|Bentley Supergroup|44109|5|Briefly described|p2 Fig. 2, p117|||Includes the Tollu Group and other mainly felsic volcanic rocks, namely the Skirmish Hill, Palgrave and Scamp volcanic associations. Mafic to felsic volcanic rocks. See also p9.||||||
1491|Bentley Supergroup|44139|5|Briefly described|p275, p283-284, p285 Fig. 3-69, p286|||Daniels (1974). ~8800 m. Southeastern Paterson Orogen; formerly referred to as Musgrave Block. Low grade metamorphosed volcanic and sedimentary rocks; also three large, cauldron-subsidence complexes of acid volcanics and granite (age relationship discussed). Includes Pussy Cat, Tollu, Cassidy, Mission Groups. Overlain by Townsend Quartzite.| | ||||05-MAR-18
1491|Bentley Supergroup|45149|6|Mentioned|p22|||||||||
1491|Bentley Supergroup|49833|5|Briefly described|p8|||||||||
1491|Bentley Supergroup|50607|6|Mentioned|p1.1, 3.2|||Geological Province: Musgrave Block.||||||
1491|Bentley Supergroup|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050 Ma. Geological Province: Musgrave Block. Equivalent to Tjauwata Group.||||||22-FEB-05
1491|Bentley Supergroup|60662|5|Briefly described|Map Legend|||Bi-modal volcanics and sediments deposited unconformably on Birksgate Complex.||||||22-FEB-05
1491|Bentley Supergroup|61154|5|Briefly described|p1, p17|Mesoproterozoic|Mesoproterozoic|Includes the Tollu Volcanics (see also Tollu Group). Geological Province: Musgrave Block.||||||03-AUG-05
1491|Bentley Supergroup|61272|6|Mentioned|p124|||||||||
1491|Bentley Supergroup|61339|5|Briefly described|Map legend|||Includes the Tollu Group (Hogarth Formation, Smoke Hill Felsic Volcanics, Mummawarrawarra Basalt and Macdougall Formation).||||||21-SEP-05
1491|Bentley Supergroup|61732|6|Mentioned|p84|||||||||07-FEB-11
1491|Bentley Supergroup|61733|5|Briefly described|p46|||Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|||||Bimodal volcanics and associated rift sediments.|
1491|Bentley Supergroup|62453|6|Mentioned|p13, 15|||Underlies: Townsend Quartzite. Of the Musgrave Complex.  Age 1080-1060Ma.||||||25-JUL-06
1491|Bentley Supergroup|62989|5|Briefly described|p39, p40|||Includes the Tollu Group (Mummawarrawarra Basalt,  Smoke Hill Volcanics and Hogarth Formation).  In W.A.||||||25-JAN-10
1491|Bentley Supergroup|63465|5|Briefly described|p553 Fig. 2|||Mafic to felsic volcanic rocks.||||||30-JAN-08
1491|Bentley Supergroup|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes Tollu Group.||||||
1491|Bentley Supergroup|63866|5|Briefly described|p202-p203, p205, p207, p212|||Musgrave Province. Synchronous with the Giles Event.|||Includes the Townsend Quartzite, Dean Quartzite, Mission Group, Cassidy Group, Pussy Cat Group, Tjauwata Group and Tollu Group and the Smoke Hill Volcanics.||Basalt, rhyolite, rhyodacite and lesser dolomite and conglomerates.|
1491|Bentley Supergroup|64580|6|Mentioned|map legend|||||||||
1491|Bentley Supergroup|64722|6|Mentioned|p17|Stenian|Stenian|Equivalent of Tollu Group therefore Stenian age inferred.||||||
1491|Bentley Supergroup|64725|6|Mentioned|p64.|||Bimodal volcanic rocks.|||Includes Tollu and Cassidy Groups.|||
1491|Bentley Supergroup|64745|6|Mentioned|p379|||Includes extrusive rocks.||||||
1491|Bentley Supergroup|65102|6|Mentioned|p364|Mesoproterozoic|Mesoproterozoic|Includes Cassidy and Mission Groups. ||||||
1491|Bentley Supergroup|65135|5|Briefly described|p6 Fig.4, p16, p18|Stenian||Regionally extensive. Includes Kunmarnara and Tollu Groups. Felsic and mafic volcanics and volcaniclastic rocks and interlayered sedimentary rocks||||||
1491|Bentley Supergroup|65256|5|Briefly described|piii, p4, p13-14|Neoproterozoic|Neoproterozoic|Blackstone region. Divided into 4 groups; includes Smoke Hill Felsic Volcanics, Tollu Group, Pussy Cat Group. A succession of sediments, and bimodal volcanics which are coeval with Giles Complex. The Tollu Group can be correlated with Tjauwata Group.||||||
1491|Bentley Supergroup|65455|6|Mentioned|p5|||Uraniferous samples in the Musgrave Province occur in granitic basement to this Supergroup.||||||09-MAY-12
1491|Bentley Supergroup|65693|6|Mentioned|p3 Fig.1.|||||||||
1491|Bentley Supergroup|65833|5|Briefly described|p1, p6 Fig.4, p16|Stenian|Stenian|Felsic and mafic volcanic and volcaniclastic rocks and interlayered sedimentary rocks. Includes Tollu and Kunmarnara Groups.||||||
1491|Bentley Supergroup|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Age shown as >1078 Ma. Includes Kunmarnara Group, and younger Tollu Group. ||||||
1491|Bentley Supergroup|65906|5|Briefly described|p3, p4, p20|Mesoproterozoic|Mesoproterozoic|A package of felsic and mafic volcanic rocks, extruded in West Musgrave Block during the c.1080 Ma Giles Event. Is part of the Warakurna Supersuite. Includes Tollu Group.||||||
1491|Bentley Supergroup|66256|5|Briefly described|p4 Fig.3, p11 Fig.8, p16, p29 Fig.26|||In west Musgrave Province.||Warakurna Supersuite|||Bimodal (basalt and rhyolite) volcanic succession.|11-JAN-17
1491|Bentley Supergroup|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Age shown as >1078 Ma. Shown as comprising only the Kunmarnara Group in this map area.||||||
1491|Bentley Supergroup|66281|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Includes Kunmarnara Group, Skirmish Hill volcanic association and Tollu Group.|||
1491|Bentley Supergroup|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.Shown as comprising Kunmarnara Group aged > 1078 Ma, and the Skirmish Hill volcanic association and Tollu Group aged c.1075 Ma.|||Includes Kunmarnara Group, Skirmish Hill volcanic association and Tollu Group.|||
1491|Bentley Supergroup|67128|5|Briefly described|p5 Fig.3, p6-7, p11, p15|||Daniels (1974); redefined by Smithies et al. (2009). Sedimentary and volcanic succession deposited during the Giles Event in the western Musgrave Province. Thought to have formed during the Warakurna LIP magmatism.|||Kunmarnara, Tollu Groups.|||
1491|Bentley Supergroup|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Includes Kunmarnara, Tollu, Cassidy and Mount Palgrave Groups.|||
1491|Bentley Supergroup|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. |||Includes Kunmarnara, Tollu, Pussy Cat, Mount Palgrave and Cassidy Groups.||Felsic volcanic and volcaniclastic rocks; quartz-pebble conglomerate and sandstone; minor mafic volcanic rocks.|
1491|Bentley Supergroup|67375|3|Fully described|pp8-9 Fig.5, pp39-53, p230, pp298-331.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Unconformably overlay the west Musgrave Province towards the end of the 1085-1040 Ma Giles Event. Includes volcaniclastic and sedimentary rocks, as well as Warakurna Supersuite volcanics. A southern extension may underlie the Officer Basin. Correlated with Tjauwata Group (SW Northern Territory).|1078 +/- 5 - 1026 +/- 26 Ma (Sun et al. 1996).|Unit in Warakurna Supersuite.|Includes Kunmarnara, Mount Palgrave, Mission, Cassidy, Pussy Cat and Tollu Groups.||Sandstone, siltstone, chert; felsic volcanic and volcaniclastic rocks; minor mafic volcanic rocks; minor calcareous sediments; weakly to moderately deformed.|
1491|Bentley Supergroup|67553|4|Described|p1-2,11,16,18,20-21,31,34-35,39-41,44|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Bentley Basin. [Also referred to as Bentley Supersuite on p44]. Outcrop extent defines the preserved extent of Bentley Basin. Deposition occuring at ?1085-?1040 Ma (GSWA data). Minimum depositional age constrained by 1057+\-6 Ma Thomas Rhyolite. Deposited in several, spatially closely associated, semi-connected, and fault-bounded depositional areas, each of them characterized by a specific stratigraphy, structural style, and diagenetic-metamorphic history. Volcanic components of the Warakurna Supersuite are also grouped as part of the Bentley Supergroup. Associated with the Ngaanyatjarra Rift, a long-lived intracontinental rift setting. Locally strongly deformed during the Petermann Orogeny (coinciding with global Pan-African period of plate reorganisation during Gondwanan assembly). See also p7, p46,65,84,93,95.|c. 1078-1040 Ma|||Underlain unconformably by Warakurna Supersuite.|Felsic and mafic volcanic and volcaniclastic rocks, and interlayered sedimentary rocks.|06-AUG-19
1491|Bentley Supergroup|67856|6|Mentioned|p337|||||||||
1491|Bentley Supergroup|67888|6|Mentioned|p65||||||Includes Kurnmarnara Group|||
1491|Bentley Supergroup|68100|6|Mentioned|p5|||Extrusive rocks formed during Giles Event (~1080-1030 Ma)|||Includes Kunmarnara Group, Tollu Group|||
1491|Bentley Supergroup|68995|5|Briefly described|p1-5, p7-8, p10, p13, p22, p29, p31|Mesoproterozoic|Mesoproterozoic|See also p34, p58. Ngaanyatjarra rift, Bentley Basin. Age based on the Mesoproterozoic Giles Event which was responsible for the deposition of the volcanic component of this Supergroup. Largest exposure of these rocks occurs within the Talbot Sub-basin where it is approximately 12km thick. Estimated thickness of this Supergroup is about 18.6km.|c. 1085-1040 Ma||Kunmarnara, Pussy Cat, Mount Palgrave, Kaarnka, Cassidy, Mission, Tollu, Tjauwata Groups.||Bimodal volcanic rocks.|
1491|Bentley Supergroup|68996|5|Briefly described|p7, p24-25, 28-29, 32-47, 63,65,66,68|||Musgrave Province. 15km thick. Upper Bentley Supergroup described p32-33. See also pp50, 53, 54, 59.|||Includes Kunmarnara Group, Cassidy Group, Mission Group, Mount Palgrave Group, Pussy Cat Group, Tollu Group||Bi-modal volcanics, volcaniclastic and sedimentary rocks.|17-JAN-17
1491|Bentley Supergroup|69003|5|Briefly described|p4, p49-52|||Bentley Basin, West Musgrave Province, Paterson Orogen. Includes the mainly felsic extrusive rocks of the Warakurna Supersuite. Igneous units were derived from fractionation of parental mafic magmas deep in the crust.|||Kunmarnara Group.||Mainly felsic volcaniclastic rocks; also siliciclastic and minor calcareous sedimentary rocks.|
1491|Bentley Supergroup|69009|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Includes Pussy Cat Group, Mount Palgrave Group, Tollu Group, and Kunmarnara Group.|||03-APR-14
1491|Bentley Supergroup|69091|4|Described|p30 Fig.3.5, p34, p35, p39, see comments|Mesoproterozoic|Mesoproterozoic|Outcrop defines Bentley Basin. Formed during Mesoproterozoic Giles Event. Minimum depositional age constrained by intrusions. Warakurna Supersuite volcanic components are grouped into Bentley Supergroup. Thickness ~18.6 km, although never achieved in any given region. ~3.7 km basaltic and ~9 km felsic magmas. See also p52-54, p58-59, p69-71, p74-76, p80-84, p86-88, p103 Fig.5.6, p105-110, p113-115, p119 Fig.5.16, p121, p130-132, p136-139 Figs.6.4-6.6, p141-144, p146, p174 Fig.9.5, p177 Fig.9.6, p181, p183-185, p200 Fig.10.2, and p205-207.|c. 1120 Ma - c. 1078 Ma||Mission, Cassidy, Mount Palgrave, Kaarnka, Pussy Cat, Tollu, Tjauwata and Kunmarnara Groups; Warakurna Supersuite.|Overlain by Townsend Quartzite (Buldya Group); overlies Giles Suite.|Bimodal volcanics; includes volcaniclastic and sedimentary rocks. Primary magmas typically reduced and water-poor but halogen-rich.|
1491|Bentley Supergroup|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/174691.1.pdf|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Geochron record for Thomas Rhyolite (174691.1.pdf) states Bentley Supergroup consists of a voluminous package of mafic and felsic volcanic rocks extruded during the Giles Event (Glikson et al., 1996), from >1085 to c. 1040 Ma (Daniels, 1974; Edgoose et al., 2004). Rocks of the Bentley Supergroup have previously been dated at 1078+/-5 Ma by U-Pb zircon (Sun et al., 1996) (from GEOCHRON/194421.1.pdf)|||Mission Group, Kaarnka Group, Pussy Cat Group, Mount Palgrave Group, Tollu Group, Kunmarnara Group, Cassidy Group||Sandstone, siltstone, and felsic volcanic and volcaniclastic rocks; minor mafic volcanic rocks|
1491|Bentley Supergroup|69436|5|Briefly described|p21:2, 11, 14|||Western Musgrave Province and Bloods Range region. These rocks are supracrustal equivalents of the Giles Complex intrusions. This unit has recently undergone reassignment of some constituents (see Tollu and Kunmarnara Groups).|||Kunmarnara Group.|Broadly correlated with the Tjauwata Group.||12-JUL-16
1491|Bentley Supergroup|69655|4|Described|p2, p5-p6, p24, p30|Stenian|Stenian|See also p31, p33-p34, p47, p57, p66, p77-p78. Musgrave Region. Magmatism associated with this supergroup is overwhelmingly dominated by mantle-derived tholeiitic mafic magmas and their felsic derivatives. Mistakenly referred to as the Bentley Supersuite on p66. Geochemistry and mineralisation potential discussed in some detail.|c. 1073 -1068 Ma||Includes the Glyde Formation, Kunmarnara Group, Pussy Cat Group, Mount Palgrave Group, Kaarnka Group, Cassidy Group, Tollu Group and the Mission Group.||Tholeiitic mafic intrusive rocks, dacites, felsic volcanics.|
1491|Bentley Supergroup|69729|4|Described|p66 Fig.1, p67-70, p79-80, p82|||Talbot Sub-basin, Musgrave Province. Up to 12km thick. The main component of this unit comprises volcanic material from the Warakurna Supersuite; their outcrop range defines the Bentley Basin. Appears as Bentley Supersuite on p67.|||Kunmarnara, Kaarnka, Mount Palgrave, Pussy Cat, Cassidy and Mission Groups.|Is intruded by the syn-volcanic Winburn Granite.|Comprises rhyolite (50%), basalt (20%) and siliciclastic to volcaniclastic rocks (30%).|
1491|Bentley Supergroup|70083|6|Mentioned|p206-207|||Musgrave Inlier. Associated with the Giles Event.|1085-1020? Ma.||||Bimodal volcanics, pyroclastic and sedimentary rocks.|
1491|Bentley Supergroup|70084|5|Briefly described|p219-220|Stenian|Stenian|Geological province: Musgrave Province, Paterson Orogen. Associated with Giles Event, and emplacement of the Kullal Dykes and Gles Intrusions; correlable to Moodini granite in the Madura province.||Unit of Warakurna Supersuite.||||
1491|Bentley Supergroup|70095|5|Briefly described|p17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin.||Unit of Warakurna Supersuite.|Includes Mission Group, Cassidy Group, Pussy-Cat Group and Mount Palgrave Group.|Uppermost unit of Warakurna Supersuite. Overlain by Buldya Group. Underlain by Winburn granite or Giles intrusions or Kunmarnara Group.||
1491|Bentley Supergroup|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Kunmarnara, Mount Palgrave, Pussy Cat, Cassidy Groups.|||
1491|Bentley Supergroup|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Mount Palgrave, Pussy Cat, Cassidy and Mission Groups.|||
1491|Bentley Supergroup|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Includes Kunmarnara Group.|||03-JUN-16
1491|Bentley Supergroup|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province, also called Bentley Supersuite (file 174691.1.pdf)|1026 Ma (Isotopic) - 1091 Ma (Inferred)|Warakurna Supersuite|Includes Cassidy Group, Kunmarnara Group, Kaarnka Group, Pussy Cat Group, Mission Group, Tollu Group||Rhyolitic and basaltic volcanic rocks, conglomerate and sandstone, and minor carbonate rock|
1491|Bentley Supergroup|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Kunmarnara Group.|||
1491|Bentley Supergroup|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Package of mafic and felsic volcanic rocks (at least 10 phases of voluminous mafic to felsic magmatism) extruded during the >1085-1026 Ma Giles Event. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1090 Ma; 1026+\-26 Ma||Includes Cassidy Group, Kaarnka Group, Kunmarnara Group, Mission Group, Pussy Cat Group, Tjauwata Group, Tollu Group.|Underlain unconformably by Warlawurru Supersuite.|Rhyolitic and basaltic volcanic rocks, conglomerate and sandstone, and minor carbonate rock|
1491|Bentley Supergroup|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. |||Tjauwata Group, Mission Group, Pussy Cat Group, Cassidy Group, Kaarnka Group, Mount Palgrave Group, Tollu Group, Kunmarnara Group,|||20-APR-20
1491|Bentley Supergroup|70831|5|Briefly described|p2-p3, p5-p6, p9|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma||Includes the Kunmaranara Group, Mount Palgrave Group, Kaarnka Group, Pussy Cat Group, Cassidy Group and Mission Group.|||
1491|Bentley Supergroup|70839|5|Briefly described|p326-327|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Emplaced within Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012).|||Includes Kunmarnara Group.|||
1491|Bentley Supergroup|71088|5|Briefly described|p4-p5|||Bentley Basin. Deposited within the structural Ngaanyatjarra Rift.|||Includes the Kunmarnara Group, Tollu Group and Tjauwata Group.|Overlain by and interbedded with the Warakurna Supersuite.||
1491|Bentley Supergroup|71169|6|Mentioned|p82|Stenian|Stenian|Musgrave Province. |1080-1040 Ma|||||
1491|Bentley Supergroup|71170|5|Briefly described|p6, p9, p44, p112, p124|Late Mesoproterozoic|Mesoproterozoic|Unconformably overlies the deformed Giles-aged layered mafic intrusions. An age of ca. 1064 Ma from Howerd et al, 2011 is provided.|c. 1075 to 1026 Ma||Includes the Tollu Group, Pussy Cat Group and the Palgrave Group.||Bi-modal volcanics.|
1491|Bentley Supergroup|71210|5|Briefly described|p8-p10, p20, p23|||Bentley Basin. See also p50, p53, p86, p131, p135.|||Includes the Kunmarnara Group and the Tollu Group.||Clastic, volcaniclastic and volcanic rocks.|
1491|Bentley Supergroup|71211|5|Briefly described|i, xiii, p4, p6, p10, p24, p26, |Mesoproterozoic|Mesoproterozoic|Intracratonic and rift dominated supergroup. See also p58, p83, p85, p135, p136 fig 4.1, p208-p209, p216, p231-p232, p234, p235.|||Includes the Pussy Cat, Cassidy, Kaarnka, Mount Palgrave, Mission, Tollu, Tjauwata and Kunmarnara Groups.||Felsic and mafic volcanics, volcaniclastic rocks and interlayered sedimentary rocks.|
1491|Bentley Supergroup|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv.|1090 Ma (inferred); 1026+\-26 Ma||Includes Cassidy Group, Kaarnka Group, Kunmarnara Group, Mission Group, Mount Palgrave Group, Pussy Cat Group, Tjauwata Group, Tollu Group.|Underlain unconformably by Wankanki Supersuite.|Rhyolitic and basaltic volcanic rocks, conglomerate and sandstone, and minor carbonate rock|
1491|Bentley Supergroup|71321|6|Mentioned|p5,11|Stenian|Stenian|Geological province: Musgrave Province. Bimodal volcanics and associated rift sediments associated with c. 1085-1040 Ma Giles Event (p11 for references).||||||
1491|Bentley Supergroup|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Mission Group, Cassidy Group, Tollu Group, Kunmarnara Group, Tjauwata Group, Kaarnka Group, Mount Palgrave Group.|||
1491|Bentley Supergroup|72094|5|Briefly described|p3 Fig 2,5-7,10-18|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Includes Mission Group, Cassidy Group, Pussy Cat Group, Mount Palgrave Group, Kaarnka Group and Kunmarnara Group and Tjauwata Group.|||
1491|Bentley Supergroup|72443|5|Briefly described|p736-738, p742-743, p746, p757, p760|Mesoproterozoic|Mesoproterozoic|Of the Musgrave Province. Stratigraphy partially drapes over the Mundrabilla Shear zone thus providing an age constraint for that structure alongside a granite south of the Musgrave region.|||Includes the Kunmarnara Group, Mount Palgrave Group, Kaarnka Group, Pussy Cat Group. Cassidy Group and the Mission Group.||Rhyolitic deposits.|
1491|Bentley Supergroup|73346|6|Mentioned|p2, p5-6|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Underlain by and interbedded with extrusive rocks of the Giles Event.||||||
1491|Bentley Supergroup|73437|5|Briefly described|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|||Kunmarnara Group, Kaarnka Group, Mount Palgrave Group, Pussy Cat Group, Cassidy Group, Mission Group, Tollu Group, Tjauwata Group|||
1572|Bibra Limestone|11797|5|Briefly described|map legend|Pleistocene|Pleistocene|Shark Bay Area. Undifferentiated Bibra Limestone and Dampier Limestone also shown on map.|||||Shelly calcarenite to calcirudite; shallow marine and beach-ridge deposits; minor calcretization.|
1572|Bibra Limestone|23726|5|Briefly described|p95|Pleistocene|Pleistocene|Underlying unit Dampier Limestone. Geological Province: Carnarvon Basin.||||||
1572|Bibra Limestone|37302|6|Mentioned|p75|||||||||
1572|Bibra Limestone|38485|4|Described|p19|||||||||
1572|Bibra Limestone|40340|5|Briefly described|Table 2|||||||||
1572|Bibra Limestone|40342|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
1572|Bibra Limestone|40343|5|Briefly described|p13|||||||||
1572|Bibra Limestone|40617|6|Mentioned|p18|||||||||
1572|Bibra Limestone|41271|4|Described|p198|||||||||
1572|Bibra Limestone|41438|6|Mentioned|Fig.23|||||||||
1572|Bibra Limestone|42025|6|Mentioned|p119|||||||||
1572|Bibra Limestone|42116|5|Briefly described|Fig.1 P6|||||||||
1572|Bibra Limestone|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Dampier Limestone|Parallel bedded limestone with invertebrate macrofossils.|
1572|Bibra Limestone|69558|5|Briefly described|p24, p98|Pleistocene|Pleistocene|Originally the Bibra Formation of Logan et al (1970b). Renamed the Bibra Limestone by Van de Graaff et al (1983). May be partly equivalent to the Dampier and Depuch Limestones. Deposited during the last interglacial period of the Pleistocene. Consists primarily of beach-ridge deposits with some tidal-flat and coralline deposits.  Contains an open-marine fauna of molluscs and corals.  ||||||
1575|Bickleys Porphyry|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
1575|Bickleys Porphyry|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
1575|Bickleys Porphyry|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1575|Bickleys Porphyry|30533|4|Described|p13|||See also Table 1||||||
1575|Bickleys Porphyry|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1575|Bickleys Porphyry|32660|5|Briefly described|Table 1|||||||||
1575|Bickleys Porphyry|32728|6|Mentioned|Fig.3|||||||||
1575|Bickleys Porphyry|36885|4|Described|p171|||||||||
1575|Bickleys Porphyry|37462|4|Described|Table 4.I|||||||||
1575|Bickleys Porphyry|39889|6|Mentioned|p495|||||||||
1575|Bickleys Porphyry|42710|5|Briefly described|map legend|Proterozoic||||||||
1575|Bickleys Porphyry|42811|5|Briefly described|p9|||||||||
1575|Bickleys Porphyry|43281|5|Briefly described|Map legend||Proterozoic|||||||
1575|Bickleys Porphyry|44155|4|Described|p234 Tb.3-2, p240, p241 Tb.3-4|Paleoproterozoic|Paleoproterozoic|See also p243 Tb.3-6, p248 Tb.3-8. West Kimberley. Comagmatic with Whitewater Volcanics; Castlereagh Hill and Mount Disaster Porphyries.||Hooper Complex||Intrudes or unconformably overlies Halls Creek Group.|Dark- to light-grey quartz-feldspar porphyry, porphyritic microgranite and microgranodiorite.|
1575|Bickleys Porphyry|44366|14|Not recorded|p.10||Proterozoic|Definition on Tech.File E/52-5. Submitted.||||||
1575|Bickleys Porphyry|44367|14|Not recorded|map legend||Proterozoic|(Reprinted 1971), part of Lamboo Complex.||||||
1575|Bickleys Porphyry|48931|5|Briefly described|p25|||Correlation||||||
1575|Bickleys Porphyry|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
1575|Bickleys Porphyry|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province; Halls Creek Orogen; North Australian Craton.||Paperbark Supersuite.|||Foliated metamicromonzogranite with phenocrysts of quartz and feldspar.|
1575|Bickleys Porphyry|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv. |1862 Ma|Paperbark Supersuite|||Foliated metamicromonzogranite with phenocrysts of quartz and feldspar.|
1575|Bickleys Porphyry|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 100k_geologyp_lut.csv.|1862 Ma (inferred)|Unit of Paperbark Supersuite.|||Grey fine grained quartz feldspar porphyry and porphyritic micromonzogranite, in places foliated; a phase contains pink feldspar phenocrysts in places|
1575|Bickleys Porphyry|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen, North Australian Craton.||Paperbark Supersuite.|||Foliated metamicromonzogranite with phenocrysts of quartz and feldspar.|
1575|Bickleys Porphyry|72437|5|Briefly described|p34, p37|||Whole-rock analyses are provided.|||||Porphyry.|
1588|Big Blow Chert|22534|6|Mentioned|p9|||||||||
1588|Big Blow Chert|42221|5|Briefly described|p10|||||||||
1588|Big Blow Chert|42696|6|Mentioned|Plate 1B|||||||||
1588|Big Blow Chert|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
1588|Big Blow Chert|43162|6|Mentioned|5|||||||||
1588|Big Blow Chert|43496|6|Mentioned|6|||||||||
1588|Big Blow Chert|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Boorara Domain.||||||
1588|Big Blow Chert|65834|6|Mentioned|p7, 33|||Boorara Domain, Kalgoorlie Terrane.||||Overlies Scotia Basalt. Is overlain by Highway Ultramafics.||
1588|Big Blow Chert|73391|5|Briefly described|p194, 244, Appendices.|||Boorara Domain, Kalgoorlie Terrane.||||Overlies Lower Basalt. Is overlain by Highway Ultramafic.|Folded and deformed siliceous chert.|
1604|Big W Rhyolite|32805|6|Mentioned|p188|||||||||
1625|Bililly Formation|29690|5|Briefly described|p13|||||||||
1625|Bililly Formation|30949|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
1625|Bililly Formation|36293|6|Mentioned|p77|||||||||
1625|Bililly Formation|36872|4|Described|p71|||||||||
1625|Bililly Formation|37460|5|Briefly described|p177|||||||||
1625|Bililly Formation|38998|4|Described|p12|||||||||
1625|Bililly Formation|40336|6|Mentioned|p15|||Misspelling of Billilly ?||||||
1625|Bililly Formation|40341|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Misspelling of Billilly? Middle - Late.||||||
1625|Bililly Formation|40342|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Misspelling of Billilly? Middle to Late||||||
1625|Bililly Formation|40343|5|Briefly described|p3|||Misspelling of Billilly ?||||||
1625|Bililly Formation|44142|5|Briefly described|p328 Tb.4-5, p329|||Unconformably overlies the Western Gneiss Terrane. Is unconformably overlain by the Byro Sub-basin sequence of the Carnarvon Basin.||Basal Badgeradda Group.|||Silty sandstone, siltstone, quartz sandstone.|
1625|Bililly Formation|48823|3|Fully described|p3 Tb. 1, p9, map legend|Paleoproterozoic|Paleoproterozoic|Quartz sandstone (lower) and thin bedded, fine-grained, silty, micaceous sandstone (upper). Unconformably overlies Nilling Beds; confomrable below Woddrarrung Formation. Thickness: ~1200ft. See also p10 Tb. 2.||||||07-NOV-08
1625|Bililly Formation|61958|5|Briefly described|Map sheet 1|Neoproterozoic|Neoproterozoic|Of the Badgeradda Group.||||||21-MAR-06
1625|Bililly Formation|64580|4|Described|map legend||Mesoproterozoic|Of Badgeradda Group. Medium- to coarse-grained arkosic sandstone, locally pebbly, overlain by micaceous siltstone to silty sandstone.||||||09-DEC-08
1625|Bililly Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
1625|Bililly Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Badgeradda Basin.||Badgeradda Group|||Medium- to coarse-grained arkosic sandstone, locally pebbly, overlain by micaceous siltstone to silty sandstone.|
1639|Billidee Formation|12733|6|Mentioned|p562.|||Contains potential hydrocarbon sealing units.||||||
1639|Billidee Formation|14228|5|Briefly described|p8, p18, p21|Permian|Permian|Thickest at NW of Merlinleigh Sub-basin (380m in Quail 1). Potential sealing unit.||Wooramel Group||Overlies Moogooloo Sandstone conformably. Overlain (conformably) by Byro Group.|Carbonaceous shale and fine to coarse-grained sandstone with minor amounts of conglomerate.|
1639|Billidee Formation|22817|5|Briefly described|p5|||Wooramel Group||||||
1639|Billidee Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
1639|Billidee Formation|23310|5|Briefly described|Map legend|Artinskian|Artinskian|Of  Wooramel Group.||||||
1639|Billidee Formation|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Wooramel Group.||||||23-DEC-09
1639|Billidee Formation|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Wooramel Group.||||||
1639|Billidee Formation|23403|4|Described|p8|Early Permian|Early Permian|Of Wooramel Group.  Locally calcareous, fine-grained sandstone and siltstone with interbedded commonly carbonaceous shale.||||||24-NOV-09
1639|Billidee Formation|23726|5|Briefly described|p45|Early Permian|Early Permian|Of Wooramel Group. Overlying unit Coyrie Formation. Underlying unit Moogooloo Sandstone.||||||
1639|Billidee Formation|23815|4|Described|p281, 282|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Wooramel Group. Overlying unit: Coyrie Formation. Underlying units: Moogooloo Sandstone and Jimba Jimba Calcarenite (conformable). Max. thickness: 206 m. Fossiliferous.||||||18-APR-05
1639|Billidee Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Wooramel Group.||||||
1639|Billidee Formation|24059|5|Briefly described|p147|Permian|Permian|Of Wooramel Group. Geological Province: Carnarvon Basin.||||||
1639|Billidee Formation|24410|5|Briefly described|p137|Permian|Permian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||24-NOV-09
1639|Billidee Formation|32113|4|Described|p50|||Re sedimentology.||||||
1639|Billidee Formation|32648|6|Mentioned|p32|||Wooramel Gp.||||||
1639|Billidee Formation|33594|6|Mentioned|p37|||||||||
1639|Billidee Formation|33710|6|Mentioned|Fig.1|||Artinskian.||||||
1639|Billidee Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
1639|Billidee Formation|35105|6|Mentioned|Fig.66|||||||||
1639|Billidee Formation|36257|6|Mentioned|Table 2.1|||||||||
1639|Billidee Formation|36890|3|Fully described|p282|||||||||
1639|Billidee Formation|37294|6|Mentioned|p100|||||||||
1639|Billidee Formation|37295|4|Described|p53|||See also P51.||||||
1639|Billidee Formation|38493|4|Described|p35|||||||||
1639|Billidee Formation|39370|5|Briefly described|p35|||||||||
1639|Billidee Formation|39427|4|Described|Table 1|||||||||
1639|Billidee Formation|40617|6|Mentioned|Fig.1|||||||||
1639|Billidee Formation|41271|3|Fully described|p85|||||||||
1639|Billidee Formation|41438|6|Mentioned|p104|||||||||
1639|Billidee Formation|42116|4|Described|p27|||||||||
1639|Billidee Formation|42392|6|Mentioned|p119|||Wooramel Group||||||
1639|Billidee Formation|42462|5|Briefly described|p55|||Merlinleigh Sub-Basin, sensu Hocking 1987.||||||
1639|Billidee Formation|43255|5|Briefly described|map legend||Artinskian|of Wooramel Group.||||||
1639|Billidee Formation|43256|5|Briefly described|5-22||Permian|||||||24-NOV-09
1639|Billidee Formation|44344|14|Not recorded|p.10-11, opp.4, map||Artinskian|Artinskian in age. (G50-1).||||||
1639|Billidee Formation|44345|14|Not recorded|map legend||Artinskian|||||||
1639|Billidee Formation|44532|4|Described|p.6,7, map|||(G50-5).||||||
1639|Billidee Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
1639|Billidee Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
1639|Billidee Formation|45016|2|Defined|p.93-9||Artinskian|Tb. p.13,14,51,74,75,77,78,82,83,85,86,88-90,92,101-2,106,121,124,126,127,129,135,137,140. (F50-13, G50-1,2,5,6).||||||
1639|Billidee Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
1639|Billidee Formation|64630|6|Mentioned|p35 |||N.B. Uppermost Wooramel Group.||||||
1639|Billidee Formation|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.||Upper unit in Wooramel Group.||Overlies Moogooloo Sandstone.|Grey siltstone, fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate.|
1639|Billidee Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey siltstone, fine-grained sandstone heterolithic.|
1639|Billidee Formation|67200|5|Briefly described|p7 fig 5, p47, app 2 p5|Kungurian|Artinskian|Thermal conductivity of 2.60 W/mK||Wooramel Group||Overlies Moogooloo Sandstone, overlain by Coyrie Formation|Interbedded limestone and sandstone with coal; laminated and trough cross bedding. Fine grained heterolithic sandstone.|
1639|Billidee Formation|67373|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.||Unit in Wooramel Group.|||Grey siltstone; fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate.|
1639|Billidee Formation|67977|5|Briefly described|p481 Fig. 2|Artinskian|Artinskian|Geol. Prov: Merlinleigh Sub-basin, Southern Carnarvon Basin||Wooramel Group||||
1639|Billidee Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Wooramel Group.||Overlain by the Coyrie Formation. Underlain by the Moogooloo Sandstone.|Comprises grey siltstone, fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate.|
1639|Billidee Formation|69166|4|Described|geologyp_lut.csv|Artinskian|Artinskian|||Wooramel Group|||Grey siltstone; fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate|
1639|Billidee Formation|69182|6|Mentioned|Ch3 p55|||||||Overlies the Callytharra Formation. Overlain by the Coyrie Formation.||
1639|Billidee Formation|69547|5|Briefly described|p191,193-194|Artinskian|Artinskian|Southern Carnarvon Basin.||Unit of Byro Group.||Overlain by Coryie Formation. Underlain by Callytharra Formation/Wooramel Group.||
1639|Billidee Formation|70138|5|Briefly described|Map legend.|Permian|Permian|Southern Carnarvon Basin.||Wooramel Group.|||Grey siltstone; fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate.|
1639|Billidee Formation|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Southern Carnarvon Basin.||Wooramel Group||Overlies the Moogooloo Sandstone. Overlain by the Byro Group.||
1639|Billidee Formation|70795|4|Described|100k_geologyp_lut.csv|Artinskian|Artinskian|Also 100k_interpgeop_lut.csv|290-283 Ma|Wooramel Group|||Grey siltstone; fine- to medium-grained sandstone; lesser black shale; minor granule to pebble conglomerate.|
1639|Billidee Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, calcilutite, calcarenite, sandstone|
1639|Billidee Formation|72910|4|Described|p4 Fig.3, p7-9, p14-15, p18, p20-24.|Artinskian|Artinskian|Thickness 60-210m. Identified in Merlinleigh Sub-basin. Type section: Northern Kennedy Range, 24d06m30sS; 115d10m00sE. See also p30, p32-34, p39, p41-42. Previously included Jimba Jimba Calcarenite Member, but these rocks now included in older Callytharra Formation. Depositional environment interpreted as a tidally influenced marine shelf to offshore delta-plain.||Wooramel Group.||Conformably overlies Moogooloo Sandstone and laterally equivalent to upper Keogh Formation. Underlies Coyrie Formation.|Interbedded grey siltstone and fine silty sandstone, lesser shale, medium to coarse sandstone, conglomerate.|18-FEB-21
1693|Bingy Bingy Basalt Member|24122|5|Briefly described|p12|Cambrian|Cambrian|Of Antrim Plateau Volcanics.||||||
1693|Bingy Bingy Basalt Member|24297|5|Briefly described|p17|Middle Cambrian|Middle Cambrian|Of Antrim Plateau Volcanics. Geological Province: Wiso Basin.||||||
1693|Bingy Bingy Basalt Member|28255|3|Fully described|p83, p90|Cambrian|Cambrian|Of the Antrim Plateau Volcanics. Medium-grained porphyritic basalt; and, agglomerate, highly weathered and laterised.  Max. thickness: ~40m.  See also Table 9 (before p83) and p143 Appendix.||||||
1693|Bingy Bingy Basalt Member|32172|4|Described|p10|||Table 2. L.Cambrian||||||
1693|Bingy Bingy Basalt Member|32173|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics.  Medium porphyritic basalt with plagioclase phenocrysts.||||||16-NOV-04
1693|Bingy Bingy Basalt Member|40993|6|Mentioned|Fig.1|||||||||
1693|Bingy Bingy Basalt Member|41840|4|Described|p40|||||||||
1693|Bingy Bingy Basalt Member|41864|4|Described|p10|||||||||
1693|Bingy Bingy Basalt Member|48943|2|Defined|p100|Early Cambrian|Early Cambrian|||||||
1693|Bingy Bingy Basalt Member|60685|6|Mentioned|p17|Cambrian|Cambrian|Of the Antrim Plateau Volcanics.||||||
1693|Bingy Bingy Basalt Member|65337|6|Mentioned|p94.|||||Unit in Antrim Plateau Volcanics.||||
1693|Bingy Bingy Basalt Member|67860|4|Described|p420 Tb. 4-18, p421 fig 4-86|Early Cambrian|Early Cambrian|0-130 m thick. Type section details given. Also appears as abbreviated Bingy Bingy Member in Tb.4-18.||Antrim Plateau Volcanics||Overlain conformably by Blackfella Rockhole Member.|Glomeroporphyritic basalt.|
1693|Bingy Bingy Basalt Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Ord Basin.||Antrim Plateau Volcanics|||Glomeroporphyritic basalt.|30-JUL-15
1693|Bingy Bingy Basalt Member|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|||Antrim Plateau Volcanics|||Glomeroporphyritic basalt.|
1693|Bingy Bingy Basalt Member|69445|5|Briefly described|p30:3-4, 12, 16|Early Cambrian|Early Cambrian|Sweet et al. (1974). Southern Victoria River region. Contains a resource of barite occurring as lenticular lodes; suitable as a weighing agent for drilling mud.||Antrim Plateau Volcanics.|||Medium-grained, glomeroporphyritic (clustered plagioclase phenocrysts) and often columnar-jointed basalts.|12-JUL-16
1693|Bingy Bingy Basalt Member|69634|4|Described|100k_interpgeop_lut.csv|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny.|508-505 Ma (Inferred)|Unit of Antrim Plateau Volcanics.|||Glomeroporphyritic basalt|
1693|Bingy Bingy Basalt Member|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||505-508 Ma|Antrim Plateau Volcanics|||Glomeroporphyritic basalt.|
1693|Bingy Bingy Basalt Member|70315|5|Briefly described|p23, p26|||Kalkarindji Province. 20-30m thick.||Antrim Plateau Volcanics||Overlies the Mount Close Chert Member. Overlain by the Blackfella Rockhole Member.|Glomero-porphyritic plagioclase basalt flow with well-developed columnar-jointing.|
1693|Bingy Bingy Basalt Member|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|508-505 Ma|Unit of Antrim Plateau Volcanics.|||Medium-grained porphyritic basalt with plagioclase phenocrysts; agglomerate.  Highly weathered and laterised.|
1705|Binthalya Formation|14228|6|Mentioned|p8|Permian|Permian|||Kennedy Group||||
1705|Binthalya Formation|23174|5|Briefly described|Fig5p8||Late Permian|||||||
1705|Binthalya Formation|23311|5|Briefly described|map legend|Paleozoic|Paleozoic|Of Kennedy Group.||||||23-DEC-09
1705|Binthalya Formation|23312|5|Briefly described|map legend|||Of Kennedy Group.||||||
1705|Binthalya Formation|23403|4|Described|p8|Late Permian|Early Permian|Of Kennedy Group.||||||24-NOV-09
1705|Binthalya Formation|23726|5|Briefly described|p38|Permian|Permian|Of Kennedy Group. Underlying unit Mungadan Sandstone. Geological Province: Carnarvon Basin.||||||
1705|Binthalya Formation|23815|4|Described|p289|Kungurian|Kungurian|Formerly known as the "Binthalya Subgroup". Geological Province: Carnarvon Basin. Of the Kennedy Group. Underlying unit: Mungadan Formation (conformable). Max. thickness: 544 m.||||||18-APR-05
1705|Binthalya Formation|24044|3|Fully described|p542|Permian|Carboniferous|Of Kennedy Group.  Geological Province: Merlinleigh Sub-basin.  Maximum thickness: 544m.||||||
1705|Binthalya Formation|30545|6|Mentioned|Fig.2|||Upper Permian||||||
1705|Binthalya Formation|30547|6|Mentioned|p426|||||||||
1705|Binthalya Formation|31561|5|Briefly described|p7|||Nonmarine plant bearing sst. & siltsts.||||||
1705|Binthalya Formation|32648|6|Mentioned|p32|||Kennedy Gp.||||||
1705|Binthalya Formation|33701|6|Mentioned|Fig.1|||Kazanian||||||
1705|Binthalya Formation|33710|6|Mentioned|Fig.1|||Kazanian.||||||
1705|Binthalya Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
1705|Binthalya Formation|35282|6|Mentioned|p39|||||||||
1705|Binthalya Formation|36890|3|Fully described|p289|||Formerly Binthalya Subgroup.||||||28-APR-14
1705|Binthalya Formation|37295|6|Mentioned|Table 2|||||||||
1705|Binthalya Formation|37303|5|Briefly described|p65|||||||||
1705|Binthalya Formation|39316|6|Mentioned|Fig.2|||||||||
1705|Binthalya Formation|40617|6|Mentioned|Fig.1|||||||||
1705|Binthalya Formation|41271|3|Fully described|p104|||Fossils do not appear age-diagnostic. Formerly "B. Subgroup"||||||
1705|Binthalya Formation|41438|6|Mentioned|p105|||See also Fig.11||||||
1705|Binthalya Formation|42116|5|Briefly described|p28|||||||||
1705|Binthalya Formation|42392|6|Mentioned|Fig.1 P114|||||||||
1705|Binthalya Formation|43015|5|Briefly described|Table 1,p319|||||||||
1705|Binthalya Formation|44219|14|Not recorded|p31||Kazanian|pt of Kennedy Group.||||||
1705|Binthalya Formation|44344|14|Not recorded|p.16-17,opp.4,map|||Topmost fm of Kennedy Group. Kungurian-?Kazanian. (G50-1).||||||
1705|Binthalya Formation|44345|14|Not recorded|map legend||Kungurian|||||||
1705|Binthalya Formation|45015|5|Briefly described|map legend|Kungurian|Kungurian|Of the Kennedy Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
1705|Binthalya Formation|45016|2|Defined|p.186-8||Tatarian|Tb. at back, p.171,176,178,180,181,182,185. ?Tatarian. (G50-1).||||||
1705|Binthalya Formation|49644|5|Briefly described|Table|||||||||
1705|Binthalya Formation|50620|5|Briefly described|p191|Late Permian|Late Permian|Of the Kennedy Group. Contains alunite-rich layers within thick-bedded mudstone and siltstone units. Geological Province: Carnarvon Basin.||||||
1705|Binthalya Formation|61958|5|Briefly described|Map sheet 1|Kungurian|Kungurian|Of the Kennedy Group.||||||
1705|Binthalya Formation|64580|6|Mentioned|map legend|||Of Kennedy Group.||||||15-DEC-08
1705|Binthalya Formation|64974|5|Briefly described|p147 Fig. 5|Kazanian|Ufimian|Of Kennedy Group. Geological Province: Carnarvon Basin.||||||24-JUN-09
1705|Binthalya Formation|66189|5|Briefly described|p454, p455 Fig.2|Roadian|Roadian|Of the Kennedy Group. Overlies the Mungadan Sandstone. Alternating mud and siltstone, with minor fine sandstone. Fossiliferous, with rare body fossils.||||||
1705|Binthalya Formation|66949|5|Briefly described|p7|Roadian|Kungurian|Southern Carnarvon Basin. A Kungurian-Roadian age suggested by Mory and Backhouse (1997) for the Kennedy Group is supported by these SHRIMP ages by Lever and Fanning (2004). SHRIMP dates are on alunite altered tuff layers, and provide maximum depositional ages.|273 +/- 18 Ma and 269 +/- 16 Ma.|Unit in Kennedy Group.||||27-AUG-15
1705|Binthalya Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Kennedy Group.|||Comprises grey to black siltstone and shale; interbedded sandstone.|
1705|Binthalya Formation|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||||||
1705|Binthalya Formation|70795|4|Described|100k_geologyp_lut.csv|Guadalupian|Guadalupian|Also 100k_interpgeop_lut.csv|272-260 Ma|Kennedy Group|||Grey to black siltstone and shale; interbedded sandstone.|
1705|Binthalya Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, greywacke|
1705|Binthalya Formation|71623|5|Briefly described|p345 fig 2|Kungurian|Kungurian|Carnarvon Basin. Unknown contact with the Kennedy Group.||||||
1705|Binthalya Formation|72505|5|Briefly described|p889-p890|Wordian|Roadian|Carnarvon Basin. Correlates with the Dulhuntyispora granulata zone. Includes tuff beds.||Kennedy Group||Overlies the Mungadan Sandstone. Overlain by the Chinty Formation?||18-MAR-20
1705|Binthalya Formation|72910|4|Described|p4, p6, p17-20, p25, p34, p38, p41.|Roadian|Kungurian|Max thickness 544m. Type section is located near Venny Peak, south-west Kennedy Range - 24d50mS, 114d57mE. Age shown as Ufimian.||Kennedy Group||Conformably overlies Mungadan Sandstone.|Grey to black siltstone and shale, interbedded fine to medium sandstone.|
1720|Birdrong Sandstone|6876|6|Mentioned|p100 Fig.5.|Early Cretaceous|Early Cretaceous|||||||
1720|Birdrong Sandstone|6944|6|Mentioned|p582, p584. |Cretaceous|Early Cretaceous|Carnarvon Basin. Overlies Gneudna Formation. ||||||27-OCT-14
1720|Birdrong Sandstone|12471|5|Briefly described|p474.|Early Cretaceous|Early Cretaceous|WAPET's 1966 Onslow 1 drilling met with gas shows in this unit. See also Figs 2, 3, 4.||Unit in Winning Group.||Is overlain by Mardie Greensand Member.||27-OCT-14
1720|Birdrong Sandstone|12729|5|Briefly described|p.3, 4, 15, 28, 32, 45-46 ||Cretaceous|Transgressive, basal Winning Group. A proven aquifer, excellent reservoir characteristics, however no hydrocarbons have been encountered in wells.||Winning Group||Overlain by the Muderong Shale.||
1720|Birdrong Sandstone|12731|5|Briefly described|p590. |Cretaceous|Cretaceous|An aquifer.||Basal unit in Winning Group.|||Basal transgressive sandstone deposited in coastal to nearshore environment, overlain by marine shales, radiolarite, siltstone, calcilutite and calcarenite.|
1720|Birdrong Sandstone|13615|3|Fully described|p4-5, p6-8, p11-12, p18|Aptian|Hauterivian|Peedamullah Shelf. Productive unit in Tubridgi Gasfield. Commonly <30m thick, up to 60m thick at a maximum. Spores/Pollen Zone and Dinoflagellate zones provided. Fluorescence and gas shows in this unit encountered in Onslow 1. Porosity of this unit is provided. Rocks in Crackling 1 that were previously assigned to this unit have been reassigned to the Flacourt Formation; additionally rocks assigned to the Mardie Greensand have been reinterepted as Birdrong Sandstone. Includes rocks previously referred to as the 'Muderong Greensand' by Andrejewskis. Intersected in numerous drillholes. The type section occurs in the Western Kennedy Range; 24deg14'50"S 114deg49'50"E. Contains a diverse, but sparse range of fauna and has a diachronous deposition spanning early Hauterivian to Aptian. Deposited in a shallow marine environment. See also p19-20, p35, p38, p40-p43, p45, 46, p48-p53, p56, p58-p75, p78, p83-p88, p102 App. 3, p118 App. 5, Plates 2, 3.||Basal Winning Group||Unconformably overlies the Flacourt Formation. Overlain by the Mardie Greensand and conformably by the Muderong Shale.|Glauconitic, predominantly coarse-grained, unconsolidated sandstone.|07-FEB-19
1720|Birdrong Sandstone|14228|5|Briefly described|p5 fig 2, p9, p16, p18-19, p26|Early Cretaceous|Early Cretaceous|Sandstone laid down at shoreline following continental break-up over entire Gascoyne Platform. Excellent reservoir characteristics: the dominant aquifer in the basin. Main objective for petroleum exploration in Gascoyne Platform.||Winning Group (basal)||Overlain by Muderong Shale.|Medium-grey, fine- to coarse-grained sandstone; minor glauconite.|
1720|Birdrong Sandstone|23311|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of Winning Group.||||||23-DEC-09
1720|Birdrong Sandstone|23312|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Winning Group.||||||
1720|Birdrong Sandstone|23355|5|Briefly described|8 Fig.1|Early Cretaceous|Early Cretaceous|||||||
1720|Birdrong Sandstone|23403|4|Described|p9|Late Cretaceous|Early Cretaceous|Of Winning Group.||||||24-NOV-09
1720|Birdrong Sandstone|23535|6|Mentioned|p125 Fig 3|Barremian|Hauterivian|Overlying unit Muderong Shale (u). Geological Province: Southern Carnarvon Basin.||||||
1720|Birdrong Sandstone|23572|4|Described|p11|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Basal unit of the Winning Group. Overlying unit: Muderong Shale.||||||
1720|Birdrong Sandstone|23726|4|Described|p61|Aptian|Neocomian|Of Winning Group. Overlying unit Muderong Shale. Geological Province: Carnarvon Basin.||||||
1720|Birdrong Sandstone|23815|4|Described|p290, 295|Aptian|Neocomian|Formerly known as the "Birdrong Formation". Geological Province: Carnarvon Basin. Max. thickness: 36 m. Overlying units: Muderong Shale and Windalia Radiolarite (both conformable).||||||18-APR-05
1720|Birdrong Sandstone|23915|5|Briefly described|p518 Table 1|Cretaceous|Cretaceous|Geological Province: Southern Carnarvon Basin.||||||
1720|Birdrong Sandstone|23935|4|Described|p11 Fig.7, p12 Fig.8|Aptian|Neocomian|Of Winning Group. Conformably overlain by Muderong Shale. Grey, fine to coarse sandstone, soft pyritic mudstone, and minor glauconite and carbonaceous siltstone. Thickness: 79 m. Geological Province: Southern Carnarvon Basin.||||||
1720|Birdrong Sandstone|24085|5|Briefly described|Not recorded|Barremian||Geological Province: Carnarvon Basin||||||16-MAR-05
1720|Birdrong Sandstone|24160|5|Briefly described|p36, 39|Cretaceous|Cretaceous|Type section ~1 km S of Birdrong Spring. 20-30 m thick.||Base of Winning Group.||Is overlain conformably by Windalia Radiolarite.|Fine- to coarse-grained quartz sandstone; locally silty and pebbly.|
1720|Birdrong Sandstone|24205|5|Briefly described|p242|||Overlain by Muderong Shale.  Geological Province: Northern Carnarvon Basin.||||||
1720|Birdrong Sandstone|24246|5|Briefly described|p20|Cretaceous|Cretaceous|Geological Province: Carnarvon Basin.||||||
1720|Birdrong Sandstone|24351|5|Briefly described|Plate 4 (in pocket)|Early Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province: Exmouth Sub-basin and Gascoyne Platform/Sub-basin.||||||13-DEC-07
1720|Birdrong Sandstone|24380|5|Briefly described|p20|Cretaceous|Cretaceous|Thickness: >25m.||||||
1720|Birdrong Sandstone|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
1720|Birdrong Sandstone|24410|5|Briefly described|p132|Cretaceous|Cretaceous|Of the Winning Group. Consists of shallow-marine, commonly galuconitic, poorly consolidated sandstone to loose sand. Overlain by Windalia Radiolarite. Geological Province: Carnarvon Basin.||||||24-NOV-09
1720|Birdrong Sandstone|24591|5|Briefly described|p21|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin.||||||
1720|Birdrong Sandstone|30186|6|Mentioned|p104|||Refs to Playford et al. (in press).||||||
1720|Birdrong Sandstone|30264|6|Mentioned|p30|||Neocomian age||||||
1720|Birdrong Sandstone|32642|6|Mentioned|p76|||Oil flow in Rough Range No.1||||||
1720|Birdrong Sandstone|32648|6|Mentioned|p32|||Winning Gp.||||||
1720|Birdrong Sandstone|32649|4|Described|p26|||See also Table 1||||||
1720|Birdrong Sandstone|33627|6|Mentioned|p582|||||||||
1720|Birdrong Sandstone|34838|6|Mentioned|p2|||||||||
1720|Birdrong Sandstone|34840|6|Mentioned|p68|||||||||
1720|Birdrong Sandstone|35105|6|Mentioned|Fig.5|||||||||
1720|Birdrong Sandstone|36257|6|Mentioned|Table 2.1|||||||||
1720|Birdrong Sandstone|36266|5|Briefly described|p150|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin.||||||31-MAR-08
1720|Birdrong Sandstone|36268|6|Mentioned|p176|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Aquifer.||||||12-MAR-08
1720|Birdrong Sandstone|36331|6|Mentioned|p2|||||||||
1720|Birdrong Sandstone|36751|6|Mentioned|p488|||||||||
1720|Birdrong Sandstone|36890|3|Fully described|p295|||Birdrong Formation.||||||10-APR-08
1720|Birdrong Sandstone|36902|6|Mentioned|p22|||||||||
1720|Birdrong Sandstone|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
1720|Birdrong Sandstone|37422|6|Mentioned|p6|||||||||
1720|Birdrong Sandstone|38352|6|Mentioned|p48|||||||||
1720|Birdrong Sandstone|38482|6|Mentioned|p22|||||||||
1720|Birdrong Sandstone|38484|6|Mentioned|p8|||||||||
1720|Birdrong Sandstone|38485|4|Described|p15|||||||||
1720|Birdrong Sandstone|38732|6|Mentioned|p32|||||||||
1720|Birdrong Sandstone|38772|6|Mentioned|p50|||||||||
1720|Birdrong Sandstone|38998|4|Described|p19|||||||||
1720|Birdrong Sandstone|39158|5|Briefly described|p36|||||||||
1720|Birdrong Sandstone|39211|6|Mentioned|p58|||||||||
1720|Birdrong Sandstone|39427|4|Described|Table 1|||||||||
1720|Birdrong Sandstone|40170|6|Mentioned|p156|||||||||
1720|Birdrong Sandstone|40306|6|Mentioned|p58|||||||||
1720|Birdrong Sandstone|40340|5|Briefly described|p14|||||||||
1720|Birdrong Sandstone|40341|6|Mentioned|Map legend|Aptian|Aptian|||||||
1720|Birdrong Sandstone|40342|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
1720|Birdrong Sandstone|40343|5|Briefly described|p11|||||||||
1720|Birdrong Sandstone|40395|6|Mentioned|p316|||||||||
1720|Birdrong Sandstone|40617|6|Mentioned|p12|||||||||
1720|Birdrong Sandstone|40801|6|Mentioned|p42|||||||||
1720|Birdrong Sandstone|40992|6|Mentioned|p13|||||||||
1720|Birdrong Sandstone|41125|5|Briefly described|p41|||||||||
1720|Birdrong Sandstone|41172|6|Mentioned|p126|||||||||
1720|Birdrong Sandstone|41271|3|Fully described|p146|||||||||
1720|Birdrong Sandstone|41436|6|Mentioned|p48|||||||||
1720|Birdrong Sandstone|41438|6|Mentioned|p108|||||||||
1720|Birdrong Sandstone|41439|5|Briefly described|p122|||||||||
1720|Birdrong Sandstone|41440|4|Described|p138|||||||||
1720|Birdrong Sandstone|41441|6|Mentioned|p153|||||||||
1720|Birdrong Sandstone|41443|4|Described|p164|||||||||
1720|Birdrong Sandstone|41445|6|Mentioned|p198|||||||||
1720|Birdrong Sandstone|41446|3|Fully described|p209|||||||||
1720|Birdrong Sandstone|41732|6|Mentioned|Fig.3|||||||||
1720|Birdrong Sandstone|42116|5|Briefly described|p10|||See also Fig.1||||||
1720|Birdrong Sandstone|42441|6|Mentioned|p3||Cretaceous|||||||
1720|Birdrong Sandstone|42442|6|Mentioned|p36|||Carnarvon Basin||||||
1720|Birdrong Sandstone|42598|2|Defined|p96, p39|Aptian|Valanginian|Age: middle Neocomian (Valanginian) to Aptian.||||||05-FEB-19
1720|Birdrong Sandstone|42734|5|Briefly described|map legend|Cretaceous||||||||
1720|Birdrong Sandstone|43564|6|Mentioned|p445|||||||||
1720|Birdrong Sandstone|43711|6|Mentioned|p18||Cretaceous|||||||
1720|Birdrong Sandstone|43712|5|Briefly described|p11|||||||||
1720|Birdrong Sandstone|43722|5|Briefly described|p10-11|||||||||
1720|Birdrong Sandstone|43724|5|Briefly described|p29|||||||||
1720|Birdrong Sandstone|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
1720|Birdrong Sandstone|44344|14|Not recorded|p.25|||||||||
1720|Birdrong Sandstone|45004|14|Not recorded|p.8|||Tb.1||||||
1720|Birdrong Sandstone|45016|14|Not recorded|p.99,176||Cretaceous|||||||
1720|Birdrong Sandstone|45168|6|Mentioned|p6|||||||||
1720|Birdrong Sandstone|49942|5|Briefly described|p4 Fig.3|Early Cretaceous|Early Cretaceous|Conformably overlain by Muderong Shale. Of Winning Group. Geological Province: Gascoyne Platform.||||||
1720|Birdrong Sandstone|50023|5|Briefly described|p14|Cretaceous|Cretaceous|Max. thickness: >25m.  Geological Province: Carnarvon Basin.||||||
1720|Birdrong Sandstone|50085|5|Briefly described|p23 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||
1720|Birdrong Sandstone|60118|6|Mentioned|p29|||Oil-bearing deposits. Geological Province: Barrow Sub-basin, North Carnarvon Basin.||||||
1720|Birdrong Sandstone|60119|5|Briefly described|p25|Early Cretaceous|Early Cretaceous|Oil-bearing rocks.  Geological Province: Carnarvon Basin.||||||
1720|Birdrong Sandstone|60379|6|Mentioned|p126 fig 3|Early Cretaceous|Early Cretaceous|Dampier sub-basin, Carnarvon Basin||||||
1720|Birdrong Sandstone|60384|5|Briefly described|p243 Fig 2a, p260 table 2, p261|Early Cretaceous|Early Cretaceous|Perth and Carnarvon Basins. Several oil shows. ||Of Winning Group.||||
1720|Birdrong Sandstone|60386|5|Briefly described|p302|Early Cretaceous|Early Cretaceous|Perth Basin, Carnarvon Basin. Non-marine. Shown to include some volcanics.||||||
1720|Birdrong Sandstone|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|||||||
1720|Birdrong Sandstone|61023|5|Briefly described|p27 Fig. 12|Cretaceous|Cretaceous|Geological Province: Northern Carnarvon Basin.||||||10-APR-08
1720|Birdrong Sandstone|61811|4|Described|p3 Fig.2, p8, p9 Table 3, p13, pp17-19.|Aptian|Barremian|Northern Perth Basin. The reservoir for many petroleum accumulations in the Northern Carnarvon Basin, and the main artesian aquifer in the Southern Carnarvon Basin. Has yielded numerous plesiosaur bones. Ferruginous pisoliths occur at the weathered top of the unit.||Unit in Winning Group.||Overlies Kockatea Shale. Is overlain by Tamala Limestone and Muderong Shale.|Friable, very poorly consolidated, poorly sorted, medium- to coarse-grained quartz sandstone.|
1720|Birdrong Sandstone|62734|5|Briefly described|p1362 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin. See also the misspelt Birdrong Formation.||||||10-APR-08
1720|Birdrong Sandstone|62837|5|Briefly described|Stratigraphic columns|Neocomian|Neocomian|Age: 130-120Ma. Geological Province: Exmouth Sub-basin and Barrow Sub-basin.||||||01-MAR-10
1720|Birdrong Sandstone|63068|5|Briefly described|p46|||Overlain by Gearle Siltstone, or by Alinga Formation (southern part of basin). Geological Province: Carnarvon Basin.||||||07-FEB-08
1720|Birdrong Sandstone|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
1720|Birdrong Sandstone|64635|5|Briefly described|p4 Fig.3, p7, p11, p14, p15 Fig.13    |Aptian|Barremian|The reservoir for many petroleum accumulations in the Northern Carnarvon Basin, and the main artesian aquifer in the Southern Carnarvon Basin.||Of the Winning Group.||Overlies the Kockatea Shale.||
1720|Birdrong Sandstone|64973|4|Described|p504, p504 Fig. 2, p505 Fig. 3, p505|Hauterivian|Valanginian|Of Winning Group. Overlies unconformably Barrow Group, overlain by Mardie Greensand. Geological Province: Carnarvon Basin. Massive to bioturbated, medium to coarse-grained sandstone that is glauconitic in the upper part. Also on p508.||||||28-APR-14
1720|Birdrong Sandstone|66126|6|Mentioned|p206|Early Cretaceous|Early Cretaceous|Carnarvon Basin.||||||
1720|Birdrong Sandstone|66189|6|Mentioned|p454|Early Cretaceous|Early Cretaceous|Disconformably overlies the Carnarvon Basin.||||||
1720|Birdrong Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes light brown carbonaceous fine-grained sandstone.|
1720|Birdrong Sandstone|67200|5|Briefly described|p8 fig 6, p17 table 1|Cretaceous|Cretaceous|Thermal conductivity of 2.83 W/mK. See also p46, p50, p53, app 2 tbl 1. ||Winning Group||Unconformably overlies Wogalli Sandstone|Bioturbated, trough and parallel cross bedded sandstone; carbonaceous fine grained sandstone.|
1720|Birdrong Sandstone|67340|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|Northern Perth Basin.||Winning Group.||||
1720|Birdrong Sandstone|67784|6|Mentioned|p26|||Onshore Carnarvon Basin. Up to 10m thick.||||Overlain by Muderong Shale.|Sandstone.|08-FEB-18
1720|Birdrong Sandstone|68811|6|Mentioned|p107|||||||Overlain by the Cape Range Group.||
1720|Birdrong Sandstone|69011|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Southern Carnarvon Basin.||Of the Winning Group.|||Comprises fine- to coarse-grained quartz sandstone, locally silty; commonly poorly consolidated; locally glauconitic.|
1720|Birdrong Sandstone|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
1720|Birdrong Sandstone|69182|5|Briefly described|Ch3 p8, Ch3 p12-p13|Cretaceous|Cretaceous|Carnarvon Basin. Deposited as part of a marine transgressive cycle. Maximum thickness greater than 160m. Forms a good quality reservoir unit and is the principal reservoir for the Tubridgi Gas Field. Sealed by the Muderong Shale. See also Ch3 p19-p20, Ch3 p23-p27, Ch3 p29-p31, Ch3 p34, Ch3 p35, Ch3 42, Ch3 p50, Ch3 p54, Ch3 p63, Ch3 p65-p66, Ch3 p69-p71, Ch3 p73, Ch4 p83.||Winning Group||Overlain by the Muderong Shale.|Sandstone.|
1720|Birdrong Sandstone|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.||||
1720|Birdrong Sandstone|69297|5|Briefly described|p247, p249, p251|Barremian|Hauterivian|Southern Carnarvon Basin. Deposited during a marine transgressive cycle. ||Winning Group||Unconformably overlies the Woodleigh Formation. Overlain by the Muderong Shale.|Sandstone.|
1720|Birdrong Sandstone|69558|6|Mentioned|p3, p258 fig 419|Early Cretaceous|Early Cretaceous|Groundwater source. Supplies a number of artesian and subartesian bores.||||Overlies and is faulted against the Wogatti Sandstone. Overlain by the Muderong Shale.||24-MAY-21
1720|Birdrong Sandstone|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Valanginian|Valanginian|See also Regional: Fig.6; p6, p9. Northern Carnarvon Basin. Supplied the first flow of oil to the surface in Australia in 1953 at Rough Range 1.||Winning Group.||Overlies Forestier Claystone. Is overlain by Mardie Greensand Member (Muderong Shale).||
1720|Birdrong Sandstone|70795|4|Described|100k_geologyp_lut.csv|Aptian|Hauterivian|Also 100k_interpgeop_lut.csv|133-113 Ma|Winning Group|||Fine- to coarse-grained quartz sandstone, locally silty; commonly poorly consolidated; locally glauconitic.|
1720|Birdrong Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greensand, sandstone|
1720|Birdrong Sandstone|72910|6|Mentioned|p16.|Early Cretaceous|Early Cretaceous|Tested in 1955 by WAPET drilling work.||||||
1720|Birdrong Sandstone|73564|5|Briefly described|p1225-1226, 1229-1230, 1232-1233|Cretaceous|Cretaceous|Exmouth Plateau. Shallow-marine, shoreface deposits. Consistently 20-30m thick. Also appears as Birdrong Sandstone Formation on p1226 and p1230.||||Overlies Zeepaard Formation. Is overlain by Muderong Shale or Mardie Greensand Member.|Sandstone dominated, with minor siltstone and conglomerate.|
1721|Birdseye Limestone|45143|6|Mentioned|Fig.3|||Time-stratigraphic interpretations.||||||
1735|Birrindudu Group|14019|4|Described|p4-5|||Comprises a conformably succession of Gardiner and Coomarie Sandstones and the Talbot Well Formation. Max. thickness: 6000m. Geological Province: Birrindudu Basin.  See also p2 Fig. 1.||||||
1735|Birrindudu Group|22446|5|Briefly described|p19|Calymmian|Calymmian|Also mentioned on page 20||||||25-JUL-06
1735|Birrindudu Group|22496|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Comprises 3 formations only the oldest of which is exposed on RUBY PLAINS - Gardiner Sandstone.  Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|22716|5|Briefly described|table4, p236|Calymmian|Calymmian|Age: 1560 Ma. Unconformably overlie the Granites- Tanami Inlier and northern province of the Arunta Inlier. Correlated with Nathan Group, McArthur Basin.||||||
1735|Birrindudu Group|22777|5|Briefly described|Map|||Birrindudu Basin||||||
1735|Birrindudu Group|23117|5|Briefly described|p445|||||||||
1735|Birrindudu Group|23314|5|Briefly described|336|Mesoproterozoic|Mesoproterozoic|||||||18-NOV-08
1735|Birrindudu Group|23621|4|Described|p31|Mesoproterozoic|Mesoproterozoic|See also page 10 Table 1. Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|23622|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|23809|5|Briefly described|p3 Fig. 1, p47 Fig. 42|Proterozoic|Proterozoic|Siliciclastic platform sediments.  Correlates with Tomkinson Creek Group (Ashburton Province) and Tawallah Group (McArthur Basin).||||||17-MAR-05
1735|Birrindudu Group|24122|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|24303|6|Mentioned|p55 Appendix|||Of the Tanami region. Probable correlative of Tomkinson Creek Group.||||||
1735|Birrindudu Group|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlies Inverway Metamorphics; unconformably overlain by Limbunya Group. Geological Province: Birrindudu Basin||||||05-AUG-05
1735|Birrindudu Group|24442|5|Briefly described|p50 Fig. 1|||Includes: Gardiner Sandstone, Talbot Well Formation, Coomarie Sandstone. Geological Province: Birrindudu Basin.||||||
1735|Birrindudu Group|29804|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
1735|Birrindudu Group|29805|6|Mentioned|Table 1|||||||||
1735|Birrindudu Group|29809|5|Briefly described|p418|||||||||
1735|Birrindudu Group|29811|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
1735|Birrindudu Group|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1735|Birrindudu Group|29813|6|Mentioned|p7|||||||||
1735|Birrindudu Group|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
1735|Birrindudu Group|31361|6|Mentioned|p6|||||||||
1735|Birrindudu Group|31362|6|Mentioned|p8|||||||||
1735|Birrindudu Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1735|Birrindudu Group|32660|5|Briefly described|Table 6|||||||||
1735|Birrindudu Group|32728|6|Mentioned|p16|||||||||
1735|Birrindudu Group|33102|6|Mentioned|Fig.2|||||||||
1735|Birrindudu Group|33377|6|Mentioned|p19|||||||||
1735|Birrindudu Group|35205|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1735|Birrindudu Group|35950|6|Mentioned|p311|||||||||
1735|Birrindudu Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1735|Birrindudu Group|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
1735|Birrindudu Group|36551|6|Mentioned|Table 12|||||||||
1735|Birrindudu Group|36902|6|Mentioned|p12|||||||||
1735|Birrindudu Group|37299|6|Mentioned|p89|||See also Fig.1.||||||
1735|Birrindudu Group|37462|4|Described|Table 4.V|||||||||
1735|Birrindudu Group|38243|6|Mentioned|Fig.2|||||||||
1735|Birrindudu Group|39887|6|Mentioned|p453|||||||||
1735|Birrindudu Group|40105|6|Mentioned|Fig.3|||||||||
1735|Birrindudu Group|41125|6|Mentioned|p30|||||||||
1735|Birrindudu Group|41883|5|Briefly described|p65|||||||||
1735|Birrindudu Group|42504|5|Briefly described|p61|||||||||
1735|Birrindudu Group|43300|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1735|Birrindudu Group|43301|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1735|Birrindudu Group|43303|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1735|Birrindudu Group|43595|4|Described|p442|||Glauconite min age: approx 1560 Ma.||||||25-JUL-06
1735|Birrindudu Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
1735|Birrindudu Group|45140|2|Defined|p12-14, p17-18, p20, p22-23, p32, p39-40|||See also p43-44, p52-56, p62, p74, p77, Appx.p15-16. Blake et al. (1975). Birrindudu Basin. Named after Birrindudu homestead. Moderately to gently folded. Up to c.6000 m thick. Hosts U and associated rare earths in the Killi Killi Hills, S of the Gardner Range. Probably marine, mainly shallow-water, sediments. May correlate with Limbunya Group, Mount Parker Sandstone and Bungle Bungle Dolomite; also Baines, Ima Ima, Lake Willson and Pindar Beds. This glauconite age is consistent with Rb-Sr samples dated at 1560 +/- 180 Ma in the range 1600-1400 Ma. Structures described.|1560+/-20 Ma (K-Ar age).||Gardiner, Coomarie Sandstones; Talbot Well Formation.|Unconformably overlies Killi Killi, Nongra and Mount Charles Beds, Pargee and Supplejack Downs Sandstones. Is overlain unconformably by Redcliff Pound Group and Antrim Plateau Volcanics.|Predominantly sublithic arenite and quartz arenite, although the middle unit contains much stromatolitic chert.|
1735|Birrindudu Group|45148|6|Mentioned|p8|||||||||
1735|Birrindudu Group|45167|5|Briefly described|Fig.27|||||||||
1735|Birrindudu Group|46788|6|Mentioned|p1|||Refers Blake et al. (1975)||||||
1735|Birrindudu Group|46864|4|Described|p37|||||||||
1735|Birrindudu Group|48950|2|Defined|p33|Neoproterozoic|Neoproterozoic|||||||
1735|Birrindudu Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Birrindudu Basin.||||||07-FEB-11
1735|Birrindudu Group|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Coomarie Sandstone, Talbot Well Formation,  Gardiner Sandstone, Supplejack Downs Sandstone.||||||07-NOV-08
1735|Birrindudu Group|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Coomarie Sandstone, Talbot Well Formation,  Gardiner Sandstone, Supplejack Downs Sandstone.||||||07-NOV-08
1735|Birrindudu Group|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Coomarie Sandstone, Talbot Well Formation,  Gardiner Sandstone, Supplejack Downs Sandstone.||||||07-NOV-08
1735|Birrindudu Group|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Basalt; sandstone; stromatolitic chert, cherty arenite, quartz arenite, siltstone, shale.||||||07-NOV-08
1735|Birrindudu Group|60685|5|Briefly described|p4 Figure 3|Proterozoic|Proterozoic|Correlated with the Tolmer Group. Geological Province: Birrindudu Basin. See also p5 Table 2.||||||19-MAY-05
1735|Birrindudu Group|61056|5|Briefly described|p778|Mesoproterozoic|Mesoproterozoic|Includes the Gairdner Sandstone. Geological Province: The Granites-Tanami Block.||||||
1735|Birrindudu Group|61861|3|Fully described|p22-24, p3 Table 1, p4, 10, 12, Map 1|Statherian|Statherian|Sediments deposited on a subdued landscape after deformation of underlying rocks. Duplication of stratigraphy through faulting seems to be common. Thickness c.1900 m. Correlated with Bastion Group in WA and Tomkinson Creek Group in Tennant Inlier.|<1800 Ma, but poorly constrained||Includes basal Gardiner Sandstone, Talbot Wells Formation, Coomarie Sandstone and now also Supplejack Downs Sandstone.|Unconformably overlies Browns Range Metamorphics, MacFarlane Peak and Tanami Groups, Pargee Sandstone and Nanny Goat Volcanics. Is overlain by Antrim Plateau Volcanics and Redcliff Pound Group.||
1735|Birrindudu Group|62377|5|Briefly described|p5, 7|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Pargee Sandstone.||||||07-NOV-08
1735|Birrindudu Group|62580|5|Briefly described|p10|||Platform sequence dominated by quartz arenite with minor carbonate. Thickness: 2km.||||||07-FEB-11
1735|Birrindudu Group|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin.||||||07-NOV-08
1735|Birrindudu Group|63261|3|Fully described|p7, p9 Fig. 5, p16-17|Paleoproterozoic|Paleoproterozoic|Comprises basal Gardiner Sandstone, Talbot Well Fm + Coomarie Sandstone, as well as Supplejack Downs Sandstone (formerly of Ware Group). Unconformable on Pargee Sandstone. Inferred age: 1735-1640Ma. Thickness: ~1900m. In Victoria-Birrindudu Basin.||||||07-FEB-11
1735|Birrindudu Group|63866|5|Briefly described|p92|||Tanami Region.||||Overlies the Pargee Group.||
1735|Birrindudu Group|64277|6|Mentioned|Map ledgend|Paleoproterozoic|Paleoproterozoic|Includes Gardiner Sandstone.||||||
1735|Birrindudu Group|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Sandstone, siltstone, shale, conglomerate, stromatolitic chert, limestone, and glauconitic sandstone.||||||09-DEC-08
1735|Birrindudu Group|64662|5|Briefly described|p28, p30 Fig. 3|Statherian|Statherian|Includes Gardiner Sandstone, Talbot Well Formation and Coomarie Sandstone. Maximum age ~1.77 Ga,  from Gardiner Sandstone. Marine to fluvial sandstone, conglomerate, and calcareous sedimentary rocks. Geological Province: Tanami region.||||||07-FEB-11
1735|Birrindudu Group|64675|5|Briefly described|p9, p10, Maps1, 4, p14, Fig.18, pp15-17|Paleoproterozoic|Paleoproterozoic|Cover sequence. See also misspelt Birrindudu Suite, Fig.6.|||Includes the Gardiner Sandstone.|Unconformably underlain by the Browns Range Metamorphics, MacFarlane Peak Group, Tanami Complex, and Coomarie Suite.|Siliciclastics.|19-MAR-14
1735|Birrindudu Group|64722|5|Briefly described|Fig. 2 p3-6, p10|Statherian|Statherian|Minimum age of 1640-1635 Ma from overlying Limbunya Group. Maximum age inferred from unconformably underlying Pargee Sandstone.||||Underlies Limbunya Group. Overlies Pargee Sandstone unconformably.||11-APR-12
1735|Birrindudu Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Birrindudu Basin unit deposited during the Calvert Event (~1730-1690 Ma)||||||
1735|Birrindudu Group|64725|6|Mentioned|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||||||
1735|Birrindudu Group|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p174 Fig.6, p175|Statherian|Statherian||1735-1640 Ma.||Includes Gardiner Sandstone.|Unconformably overlies Pargee Sandstone.||20-APR-12
1735|Birrindudu Group|64734|6|Mentioned|p186 Fig.1|||||||||14-SEP-09
1735|Birrindudu Group|64737|5|Briefly described|p232 Fig.2, p233, p243-4|||Correlated with Reynolds Package in this paper.|||Includes Gardiner Sandstone.|Unconformably overlies Tanami Group.|Sandstone-dominated succession with some carbonate and mudstone in the upper part.|30-APR-12
1735|Birrindudu Group|64748|5|Briefly described|p275|Statherian|Statherian|In the Birrindudu Basin; correlated with the Bastion Group; given ages between 1790-1700Ma and 1735-1640Ma||||||
1735|Birrindudu Group|65074|5|Briefly described|p349-352, p354-355, p362|Mesoproterozoic|Mesoproterozoic|In Northern Birrindudu Basin. Up to 6km thick. Correlates with Limbunya Group.|c.1.6 Ga.||Gardiner Sandstone, Talbot Well Formation, Coomarie Sandstone.|Unconformably overlain by Redcliff Pound Group and Antrim Plateau Volcanics.|Siliciclastic with some carbonate: see components' lithologies.|
1735|Birrindudu Group|65232|5|Briefly described|p78|||Correlatives of Katherine River Group and Tolmer Group. Dominated by shallow-marine sedimentary rocks. Geol. Prov: Tanami Region.||||||18-FEB-10
1735|Birrindudu Group|65323|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65324|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Platform cover sequence 1. Age given as: ~1790-1750Ma.||||||02-MAR-10
1735|Birrindudu Group|65326|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65327|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone.  Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65328|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||
1735|Birrindudu Group|65338|6|Mentioned|p21.|||Claoue-Long et al. (2008a) have suggested a correlation between this unit and Reynolds Range Group.||||||
1735|Birrindudu Group|65339|6|Mentioned|p5 Fig.4. ||||||||Sandstone, conglomerate, greywacke.|
1735|Birrindudu Group|65342|5|Briefly described|pp10-11.|||Birrindudu Basin.|||Includes Gardiner and Coomarie Sandstones and Talbot Well Formation.|Unconformably overlies Inverway Metamorphics. Is unconformably overlain by Limbunya Group.|Mostly coarse siliciclastic sedimentary rocks.|
1735|Birrindudu Group|65349|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Platform cover sequence 1. Age given as: ~1790-1750Ma.||||||02-MAR-10
1735|Birrindudu Group|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Platform cover sequence 1. Age given as: ~1790-1750Ma.||||||
1735|Birrindudu Group|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone and Supplejack Downs Sandstone. Platform cover sequence 1. Age given as: ~1790-1750Ma.||||||
1735|Birrindudu Group|65352|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65353|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65354|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone; Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone.  Age given as ~1790-1750 Ma?||||||
1735|Birrindudu Group|65355|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65356|5|Briefly described|Map legend|Statherian|Statherian|Includes the Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone, Supplejack Downs Sandstone. Age given as ~1790-1750 Ma?||||||02-FEB-10
1735|Birrindudu Group|65358|5|Briefly described|p7, p10|Late Paleoproterozoic|Late Paleoproterozoic|Includes Helena Creek beds. Platform cover succession.||||||
1735|Birrindudu Group|66129|5|Briefly described|p213, p216 Fig.3|Calymmian|Statherian|1735-1640 Ma. Contains Gardiner Sandstone. Unconformably overlies Pargee Sandstone.||||||
1735|Birrindudu Group|66468|5|Briefly described|p19, p20, p21 Fig.6, p24 Fig.7|Neoproterozoic|Mesoproterozoic|Unconformably overlies Pargee Sandstone. ~6km thick, sandstone, siltstone, shale and carbonate. Contains Gardiner Sandstone.||||||
1735|Birrindudu Group|66860|6|Mentioned|p6 Tb.1|||Tanami Region.||||||
1735|Birrindudu Group|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Supplejack Downs, Gardiner and Coomarie Sandstones and Talbot Well Formation.|Unconformably overlies Tanami and Mount Winnecke Groups, Pargee Sandstone, Coomarie Suite and Mount Charles Formation. Is unconformably overlain by Antrim Plateau Volcanics.||
1735|Birrindudu Group|67824|6|Mentioned|p385 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||
1735|Birrindudu Group|67826|6|Mentioned|p401 Fig.2, p403|Paleoproterozoic|Paleoproterozoic|Relatively flat-lying sedimentary rocks.|~ 1770-1640 Ma|||||
1735|Birrindudu Group|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.||||||
1735|Birrindudu Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Statherian|Statherian|Birrindudu Basin. See also 500k_geologyp08_lut.|||||Conglomerate, cross-bedded sandstone, wacke, siltstone, mudstone and shale; minor fine-grained micaceous quartz sandstone; stromatolitic chert, limestone, and glauconitic sandstone.|25-NOV-15
1735|Birrindudu Group|68733|5|Briefly described|p177, p186, p187 Fig.6|Statherian|Orosirian|Birrindudu Basin. Does not crop out in this study area. Uncertain correlation with Limbunya Group discussed.|ca. 1812 Ma (maximum depositional age).||Includes Coomarie Sandstone.|Unconformably overlain by the Limbunya Group. Unconformably underlain by the Pargee Sandstone.|Siliciclastic dominated.|04-DEC-17
1735|Birrindudu Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
1735|Birrindudu Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Statherian|Statherian|Birrindudu Basin|||Includes Gardiner Sandstone||Sublithic arenite, quartz arenite, siltstone, shale, conglomerate, stromatolitic chert, limestone, and glauconitic sandstone.|30-JUL-15
1735|Birrindudu Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.|||Includes Gardiner Sandstone||Sublithic arenite, quartz arenite, siltstone, shale, conglomerate, stromatolitic chert, limestone, glauconitic sandstone|
1735|Birrindudu Group|69182|6|Mentioned|Ch4 p3|||Canning Basin. ||||||
1735|Birrindudu Group|69253|5|Briefly described|p746, p747 Fig.1|Neoproterozoic|Mesoproterozoic|~6 km thick. Marine to fluvial sediments. Appears as Birrindudu Formation on p746.||||Unconformably overlies Pargee Sandstone.|Sandstone, shale, carbonate.|
1735|Birrindudu Group|69417|6|Mentioned|p2:5-6|Statherian|Statherian|Southern Birrindudu Basin. Represents part of a single, large un-named superbasin linked at depth beneath overlying basins.||||||12-JUL-16
1735|Birrindudu Group|69425|6|Mentioned|p10:4|||Mentioned as possible correlative of Hatches Creek Group, based on geochronological grounds.||||||12-JUL-16
1735|Birrindudu Group|69426|5|Briefly described|p11:5 Fig.11.4, 11:8-9, 14-15|||In Blake et al. (1979). Is disrupted by the Black Peak Fault.|||Gardiner, Supplejack Downs, Coomarie Sandstones; Talbot Well Formation.|Unconformably overlies Ware Group and Mount Charles Formation.||12-JUL-16
1735|Birrindudu Group|69429|5|Briefly described|p14:1|||||||Unconformably overlies Inverway Metamorphics.|Includes interbedded mudstone and siltstone.|12-JUL-16
1735|Birrindudu Group|69431|6|Mentioned|p16:1|||||||Age-equivalent of Reynolds Range Group.||12-JUL-16
1735|Birrindudu Group|69432|4|Described|p17:2-6, 12-13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Estimated thickness c.1900-6000m. Unmetamorphosed and only gently dipping. Is overlain unconformably by Limbunya and Redcliff Pound Groups, Kalkarindji Suite, Lucas Formation, Pedestal Beds and Larranganni beds. Age is not well-constrained. The basal conglomerate rests on granite dated at 1794 +/- 4 Ma; the unconformably underlying Pargee Sandstone has detrital zircons aged 1768 +/- 14 Ma which is thus the maximum deposition age for the Group. Other age determinations detailed.|<1768 Ma.||Gardiner, Coomarie Sandstones; Talbot Well Formation.|Unconformably overlies Inverway Metamorphics, Tanami and Ware Groups, Pargee Sandstone, Grimwade and Frederick Suites. See Comments for overlying units.||12-JUL-16
1735|Birrindudu Group|69435|6|Mentioned|p20:1|||Birrindudu Basin. Possible correlative of the Fitzmaurice Group.||||||12-JUL-16
1735|Birrindudu Group|69440|6|Mentioned|p25:1|||Birrindudu Basin.||||||12-JUL-16
1735|Birrindudu Group|69587|4|Described|GEOL_LUT_CSV files|Statherian|Statherian|Geological province: North Australian Craton. Of Birrindudu Basin. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 2_5m_geologyp98_lut.csv.|1735-1640 Ma (inferred)||Includes Gardiner Sandstone.||Conglomerate, cross-bedded sandstone, siltstone, mudstone and shale|
1735|Birrindudu Group|69597|6|Mentioned|p5 fig 2b|||||||||
1735|Birrindudu Group|69618|6|Mentioned|p90, p100 Fig.10|Paleoproterozoic|Paleoproterozoic|||||||
1735|Birrindudu Group|69634|4|Described|GEOL_LUT_CSV files|Statherian|Statherian|Of Birrindudu Basin. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1735-1640 Ma (Inferred)||Includes Gardiner Sandstone.||Undivided; sandstone, siltstone, shale, conglomerate, stromatolitic chert, limestone, and glauconitic sandstone|
1735|Birrindudu Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35, p49|Statherian|Statherian|6km thick. Deposition occurred between 1768 - 1640 Ma.||||Unconformably overlain by Limbunya Group, correlated with Tawallah Group||
1735|Birrindudu Group|69747|6|Mentioned|p263|||Geological province: Tanami Block, North Australian Craton.||||||
1735|Birrindudu Group|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Gardiner Sandstone.|||
1735|Birrindudu Group|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|1735-1640 Ma.||Gardiner Sandstone.|Overlies Killi Killi Formation. Is overlain by Redcliff Pound Group.|Conglomerate, wacke, sandstone, siltstone, mudstone, shale.|
1735|Birrindudu Group|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|1735-1640 Ma.||||Cross-bedded sandstone, siltstone and shale.|
1735|Birrindudu Group|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Unclear if age range refers to the Group or just the Gardiner Sandstone.|1735-1640 Ma.||Gardiner Sandstone.|||
1735|Birrindudu Group|70154|4|Described|500k_interpgeop14_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|1640-1735 Ma||||Sublithic arenite, quartz arenite, siltstone, shale, conglomerate, stromatolitic chert, limestone, and glauconitic sandstone.|
1735|Birrindudu Group|70291|4|Described|p178,180-181|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Coeval with D6+ event (Late thrust, oblique-slip and normal faults that cut earlier structures; ages poorly constrained, but likely <1,700 Ma, possibly as young as the Alice Springs Orogeny (450-300 Ma)).|ca. 1735-1640 Ma||Includes Coomarie Sandstone, Talbot Wells Formation, Gardiner Sandstone.||Sandstone, siltstone, shale, and carbonate|24-JUN-19
1735|Birrindudu Group|70731|6|Mentioned|p268,278|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
1735|Birrindudu Group|70826|6|Mentioned|p5 tbl 2, p9, p10|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. May be a correlative of Hidden Basin beds.||||||15-MAY-20
1735|Birrindudu Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Gardiner, Coomarie Sandstones; Talbot Well Formation.|Unconformably overlies Tanami Group.||
1735|Birrindudu Group|70851|6|Mentioned|p19, p29|||||||||
1735|Birrindudu Group|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.|||Gardiner Sandstone, Talbot Well Formation.|||
1735|Birrindudu Group|71080|6|Mentioned|p26|||Birrindudu Basin.||||Equivalent to Hidden Basin beds?||
1735|Birrindudu Group|71169|5|Briefly described|p71|Statherian|Statherian|North Australian Craton.|c. 1800-1700 Ma|||||
1735|Birrindudu Group|71171|6|Mentioned|p6|||||||Unconformably overlain by the Carranya Formation.||
1735|Birrindudu Group|71267|4|Described|GEOL_LUT_CSV files|Statherian|Statherian|Geological province: Granites-Tanami Orogen. Of Birrindudu Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv and geochron files.|1735-1640 Ma (inferred)||Includes Gardiner Sandstone, Coomarie Sandstone, Talbot Well Formation.|Underlain unconformably by Browns Range Metamorphics.|Sandstone, lesser siltstone, shale, and conglomerate; minor stromatolitic chert, limestone|
1735|Birrindudu Group|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.|||Includes Coomarie Sandstone, Talbot Well Formation, Gardiner Sandstone.|Overlain by Limbunya Group. Equivalent to Tolmer Group.||
1735|Birrindudu Group|71349|5|Briefly described|p724-725, p727|Paleoproterozoic|Paleoproterozoic|Tanami Region. Relatively flat-lying sedimentary rocks.|1735-1640 Ma.||Gardiner Sandstone, Talbot Well Formation, Coomarie Sandstone.|||
1735|Birrindudu Group|71397|6|Mentioned|p5|Statherian|Statherian|Geological province: Granites-Tanami Orogen.||||||
1735|Birrindudu Group|72034|5|Briefly described|500k_interpgeop16_lut|Statherian|Statherian|Birrindudu Basin.|||||Sandstone, lesser siltstone, shale, and conglomerate; minor stromatolitic chert, limestone.|
1735|Birrindudu Group|72071|5|Briefly described|p1297-1298,1301-1303|Proterozoic|Proterozoic|6 km thick.|||Includes Gardiner Sandstone.|Underlain unconformably by Browns Range Metamorphics.|Sandstone|
1735|Birrindudu Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Tawallah Group (central/southern McArthur Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
1735|Birrindudu Group|72718|6|Mentioned|p12|||||||||
1737|Biscay Formation|22496|3|Fully described|p7|Orosirian|Orosirian|1880 +/- 3 Ma, Halls Creek Group, Halls Creek Province. Overlain by Olympio Formation||||||
1737|Biscay Formation|22526|3|Fully described|P679, P680, Fig2||Orosirian|Age of unit is 1880+/-3 Ma.||||||09-DEC-08
1737|Biscay Formation|22547|5|Briefly described|p14|Orosirian|Orosirian|Of the Halls Creek Group. Age: 1880 +/- 3 Ma.||||||14-NOV-06
1737|Biscay Formation|22716|6|Mentioned|p234|||||||||
1737|Biscay Formation|22754|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group. Age c. 1880 Ma.||||||07-NOV-08
1737|Biscay Formation|22777|5|Briefly described|Map|||||||||
1737|Biscay Formation|23205|6|Mentioned|p42|Paleoproterozoic|Paleoproterozoic|of Halls Creek Inlier.||||||07-NOV-08
1737|Biscay Formation|23383|6|Mentioned|p9, p12|||Of Halls Creek Group. Part of these rocks have been reclassified as Koongie Park Formation (originally proposed as Koongie Park Member, a component of Tickalara Metamorphics).Age: 1880 Ma (SHRIMP).||||||25-JAN-05
1737|Biscay Formation|23599|4|Described|p9|Paleoproterozoic|Paleoproterozoic|Age: c.1880 Ma (SHRIMP U-Pb-zircon). Of Halls Creek Group. Overlying unit Olympio Formation. Underlying unit Saunders Creek Formation. Max. thickness: 1500 m.||||||07-NOV-08
1737|Biscay Formation|23621|3|Fully described|p15|Orosirian|Orosirian|See also p11 table 1. Age: 1880+/-2 Ma. Of Halls Creek Group. Overlying unit Olympio Formation. Underlying unit Saunders Creek Formation. Halls Creek Orogen. Max. thickness: >1000 m.||||||
1737|Biscay Formation|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group.||||||07-NOV-08
1737|Biscay Formation|24173|3|Fully described|p16, p13 Tb.2|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Gp. Mafic and subordinate felsic volcanics, clastics, carbonates, chert. Conformable under Olympio Fm; conformable over Saunders Creek Fm. Geol.Prov: Halls Creek Orogen. Max Thickness: >1000m. Age: c.1880Ma. Intruded by Woodward Dolerite||||||07-NOV-08
1737|Biscay Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group (Lamboo Complex).   Metamorphosed (low- to medium-grade) basaltic volcanic and sedimenatry rocks; interbedded with mudstone, siltstone, sandstone and carbonate rock.  Age: c. 1880Ma.||||||07-NOV-08
1737|Biscay Formation|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group.  Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
1737|Biscay Formation|29845|5|Briefly described|p120|||||||||
1737|Biscay Formation|30097|6|Mentioned|Fig.54|||Tables 23,24,26||||||
1737|Biscay Formation|30892|5|Briefly described|p94|||Archaean?||||||
1737|Biscay Formation|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1737|Biscay Formation|32660|5|Briefly described|Table 1|||||||||
1737|Biscay Formation|32728|5|Briefly described|Table 3|||||||||
1737|Biscay Formation|33443|6|Mentioned|p260|||||||||
1737|Biscay Formation|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
1737|Biscay Formation|36551|6|Mentioned|Table 15|||See also P25.||||||
1737|Biscay Formation|36885|4|Described|p166|||||||||
1737|Biscay Formation|36902|6|Mentioned|p11|||||||||
1737|Biscay Formation|37462|4|Described|Table 4.I|||||||||
1737|Biscay Formation|37577|6|Mentioned|p34|||||||||
1737|Biscay Formation|38482|6|Mentioned|Table 1|||||||||
1737|Biscay Formation|41465|5|Briefly described|p6|||||||||
1737|Biscay Formation|41594|6|Mentioned|p46|||||||||
1737|Biscay Formation|41976|4|Described|p459|||||||||
1737|Biscay Formation|41977|5|Briefly described|p471|||||||||
1737|Biscay Formation|41980|6|Mentioned|Fig.5 P587|||||||||
1737|Biscay Formation|41987|6|Mentioned|Fig.3 P73|||||||||
1737|Biscay Formation|42149|6|Mentioned|p711|||||||||
1737|Biscay Formation|42326|6|Mentioned|p9|||||||||
1737|Biscay Formation|42329|6|Mentioned|Fig.3 P15|||||||||
1737|Biscay Formation|42768|5|Briefly described|p6|||of Halls Creek Group||||||
1737|Biscay Formation|43299|5|Briefly described|Map Legend||Paleoproterozoic|of Halls Creek Group.||||||07-NOV-08
1737|Biscay Formation|43303|5|Briefly described|Map Legend||Paleoproterozoic|of Halls Creek Group. Age about 1880 Ma.||||||07-NOV-08
1737|Biscay Formation|43595|5|Briefly described|p350|||||||||
1737|Biscay Formation|43610|5|Briefly described|p19|||Age: approx. 1880 Ma||||||
1737|Biscay Formation|43632|3|Fully described|p2,Fig.1||Proterozoic|||||||
1737|Biscay Formation|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
1737|Biscay Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
1737|Biscay Formation|44155|4|Described|p234-238, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|East Kimberley. 2-3km thick. The basalt has MORB affinities. Prominent pre-tectonic mafic sills and dykes. U-Pb zircon age from a high-level felsic sill, or volcanic.|>1856 +/- 5 Ma (Page and Hancock, 1988).|||Overlies Saunders Creek Formation. Is intruded by Woodward Dolerite. Is overlain conformably (gradationally) by Olympio Formation.|Four units: phyllite and marble; overlain by rhyolite, crystal-lithic tuff, phyllite, massive amphibolite after amygdaloidal basalt; then bimodal volcanics, carbonates and ferruginous-carbonates, BIF; finally metabasalt, phyllite and calc-silicates.|
1737|Biscay Formation|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Halls Creek Group. Metamorphosed basaltic volcanic and volcaniclastic rock; minor dolerite sills and interbedded pelite; carbonate and chert lenses. Age: c.1880Ma. In the Lamboo Complex.||||||07-NOV-08
1737|Biscay Formation|44317|4|Described|Table 1|||Archaean or Proterozoic.||||||
1737|Biscay Formation|44318|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
1737|Biscay Formation|44324|14|Not recorded|p.5|Proterozoic|Archean|Tb.1. Of Halls Creek Group. (Archaean-Proterozoic).||||||07-NOV-08
1737|Biscay Formation|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
1737|Biscay Formation|44397|14|Not recorded|p.22, Table 1|||Hall Creek Group. Archaean or Proterozoic.||||||
1737|Biscay Formation|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
1737|Biscay Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
1737|Biscay Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
1737|Biscay Formation|45047|2|Defined|p63|Proterozoic|Proterozoic|||||||
1737|Biscay Formation|45048|6|Mentioned|p10|||Halls Creek Group. See also Fig.13||||||
1737|Biscay Formation|45086|5|Briefly described|p25|||Lithology.||||||
1737|Biscay Formation|45140|2|Defined|p13, p25, Appx.p12-13.|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1969). Halls Creek Province. Named after Bay of Biscay Hills. The reference area is the core of the Biscay Anticlinorium, Dixon Range sheet area. Thickness unknown due to isoclinal folding; probably 1000m.||Halls Creek Group.||Conformably overlies Saunders Creek Formation. Is overlain conformably by Olympio Formation.|Metamorphosed marine sedimentary rocks, basic volcanics and intrusive rocks.|
1737|Biscay Formation|46797|6|Mentioned|p80|||Dates given||||||
1737|Biscay Formation|50437|6|Mentioned|p5.7|||Intruded by San Sou Suite.||||||
1737|Biscay Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Halls Creek Group. Age: c. 1880Ma. Metamorphosed (low-medium grade) basaltic volcanic rock and sedimentary rock; minor metadolerite sills.||||||
1737|Biscay Formation|60724|4|Described|p4, p7|||Of the Halls Creek Group. Characterised by mafic volcanic rocks and interbedded sedimetary rocks. Overlain by the Olympio Formation. Intruded by Woodward Dolerite. Within the Lamboo Complex.||||||
1737|Biscay Formation|61056|5|Briefly described|p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1870+/-4Ma and ca1880Ma felsic volcanics.||||||07-NOV-08
1737|Biscay Formation|61861|5|Briefly described|p9, p12, Fig.2|||Eastern zone of Halls Creek Orogen. Has lithological similarities with MacFarlane Peak Group, Dead Bullock Formation.|1880 Ma (Blake et al. 1998).|?May be unit in Halls Creek Group.||Correlated with MacFarlane Peak Group. Overlies Saunders Creek Formation. Is overlain by Olympio Formation.||
1737|Biscay Formation|63866|4|Described|p130|Orosirian|Orosirian|Interpreted to have been deposited in a shallow marine setting with subaerial to subaqueous volcanism either on a passive continental margin or intracratonic setting.|c. 1880 and 1868 Ma (R. Page)|Halls Creek Group||Conformably overlies the Saunders Creek Formation.|Low-grade mafic and subordinate felsic volcanics and clastic sedimentary rocks including carbonate and chert.|
1737|Biscay Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Halls Creek Group. Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies.||||||09-DEC-08
1737|Biscay Formation|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|Of Eastern Zone of Halls Creek Orogen. Age from rhyolite of the Formation (now interpreted as part of Olympio Formation).|1856 +/- 5 Ma (Page & Hancock 1988).|||||12-APR-12
1737|Biscay Formation|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Eastern Zone of the Lamboo Complex.|||||Mafic volcanic rocks.|
1737|Biscay Formation|67127|6|Mentioned|p85||||||||Sedimentary rocks and metabasalt.|
1737|Biscay Formation|68078|6|Mentioned|p7 figure 4|Paleoproterozoic|Paleoproterozoic||~1880 Ma|||||
1737|Biscay Formation|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Paleoproterozoic|Paleoproterozoic|||Halls Creek Group|||Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies.|
1737|Biscay Formation|69003|5|Briefly described|p5, p19, p20 Fig.25|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.|c.1880 Ma.|Halls Creek Group.|||Planar parallel laminated, very fine-grained recrystallised arenite and graphitic siltstone.|
1737|Biscay Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comments: (1880Ma) 'This is a reliable igneous crystallisation age for felsic volcanism. (1870 Ma) 'Good measurement of age of magmatic zircon crystallisation; a maximum for stratigraphic age of the upper Biscay Formation.'|Crystallisation ages: 1880+/- 3 Ma, 1870+/-4 Ma|Halls Creek Group|Includes 5 unnamed members.||Basaltic and minor felsic metavolcanic and metavolcaniclastic rocks; interbedded pellite, psammite, and metacarbonate; minor metadolerite sills.|30-JUL-15
1737|Biscay Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1868-2349 Ma|Halls Creek Group|||Basaltic metavolcanic and metavolcaniclastic rocks, minor felsic metavolcanics and metavolcaniclastic rocks; interbedded pellite, psammite and metacarbonate. Minor metadolerite sills.|
1737|Biscay Formation|69585|5|Briefly described|p2, p4|Orosirian|Orosirian|Eastern Lamboo Province. Passive margin deposits.|1880 Ma.|Halls Creek Group.||Is overlain by Olympio Formation.||
1737|Biscay Formation|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Unit of Halls Creek Group.|||Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies|
1737|Biscay Formation|69597|6|Mentioned|p5 fig 2b|||||||||
1737|Biscay Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1880-1870 Ma (Isotopic)||||Basaltic and minor felsic metavolcanic and metavolcaniclastic rocks; interbedded pellite, psammite, metachert lenses and metacarbonate; commonly schistose or mylonitic, minor metadolerite sills|
1737|Biscay Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1870-1880 Ma||||Basaltic metavolcanic and metavolcaniclastic rocks, interbedded pellite, psammite and metacarbonate. Minor felsic metavolcanics and volcaniclastic rocks. Interbedded psammite and pelite.|
1737|Biscay Formation|70731|5|Briefly described|p268|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||Unit of Halls Creek Group.||||
1737|Biscay Formation|70812|4|Described|p5-p7, p11, p19, p27, p30, p38|Orosirian|Orosirian|Eastern Zone of the Halls Creek Orogen, Lamboo Province. Mineralisation is described.|c. 1880 Ma|Halls Creek Group||Overlies the Saunders Creek Formation. Overlain by the Olympio Formation.||
1737|Biscay Formation|70851|4|Described|p3-p5, p12|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.|c. 1880 Ma|Halls Creek Group||Overlies the Saunders Creek Formation. Overlain by the Olympio Formation.|Mafic volcanic rocks.|
1737|Biscay Formation|71113|5|Briefly described|p96-97|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Sedimentation and sub-aqueous to subaerial volcanism likely occurred on a passive continental margin (Sheppard et al., 1999b). SHRIMP U-Pb zircon afe og 1880+\-3 Ma from felsic metavolcanics (Blake et al., 1998).||Unit of Halls Creek Group.||Overlain disconformably by Olympio Formation/Maude Headley Member. Underlain by Saunders Creek Formation.|Massive and pillowed metabasaltic lava and fine-grained mafic volcaniclastic deposits, siliciclastic and calcareous metasedimentary rocks, and subordinate felsic metavolcanic rocks.|
1737|Biscay Formation|71140|5|Briefly described|p96-97|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen. Passive continental margin deposition with sub-aqueous to subaerial volcanism.|1880 +/- 3 Ma (SHRIMP: Blake et al., 1998).|Halls Creek Group.||Conformably overlies Saunders Formation. Is overlain disconformably by Olympio Formation.|Massive and pillowed metabasaltic lava and fine-grained mafic volcaniclastic deposits, siliciclastic and calcareous metasedimentary rocks, and subordinate felsic metavolcanic rocks.|
1737|Biscay Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1881-1861 Ma (inferred)|Unit of Halls Creek Group.||Overlain disconformably(?) by Olympio Formation. Underlain conformably by Saunders Creek Formation.|Basaltic metavolcanic and metavolcaniclastic rocks; interbedded pelite and psammite; minor metadolerite sills, metacarbonate and metachert lenses, interbedded psammite and pelite|
1737|Biscay Formation|71397|3|Fully described|p1,3-5,7-8,11,14-16,19,22-27,30,32|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Deposited in a shallow-marine environment. Based on significant differences in sedimentology and U-Pb zircon geochronology, the lower Biscay Fm has been redefined as Brim Rockhole Fm, and upper Biscay Fm is redefined as Biscay Fm. Metamorphosed to upper greenschist to lower amphibolite facies. Top of Biscay Formation is identified either by the uppermost mafic metavolcanic unit or by a chert or siliceous tuff bed overlying the uppermost mafic metavolcanic unit (Warren, 1997). Geochemical analysis of metavolcanic rocks indicate basalt or basaltic andesite affinities for metamafic rocks, and a rhyolitic affinity for metafelsic samples. See p23,25 for detailed major and trace-element geochemical analysis. Sm-Nd whole-rock isotope analysis showed CHUR-like mantle signature (ENd between -0.78 and +0.72), with a TDM2 model ages between c. 2290 and 2174 Ma. Samples GSWA 206183 and 206185 (metasandstones) yielded weighted mean 207Pb*/206Pb* dates of 1872+\-5 Ma 1872+\-6 Ma, interpreted as maximum depositional ages of sandstone protoliths.  Sample GSWA 206187 (pelitic schist) yielded a weighted mean 207Pb*/206Pb* date of 1861+\-3 Ma, interpreted as maximum depositional age of sedimentary protolith. Hafnium data indicate sediment deposition with  a mix of autochthonous and allochthonous sources. See also p36-37,42-48.|c. 1881-1861 Ma|Unit of Halls Creek Group.||Overlain disconformably to unconformably by Olympio Formation. Underlain unconformably by Brim Rockhole Formation. Intruded by Woodward Dolerite.|Thick packages of siliceous metasandstone and metasiltstone intercalated with massive basalt becoming amygdaloidal toward flow tops.|28-NOV-19
1737|Biscay Formation|71873|5|Briefly described|p426-427,443|Orosirian|Orosirian|Geological province: Lamboo Province. Depositioanl environment: shallow-marine. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|c. 1881 Ma; Blake et al., 1999|Unit of Halls Creek Group.||||
1737|Biscay Formation|72437|5|Briefly described|p7-9, p52-53|Palaeoproterozoic|Palaeoproterozoic|Mafic rocks include lava flows, pyroclastic rocks and volcaniclastic deposits. Nine whole-rock analyses are obtained for basaltic lava flows and one whole rock analysis of an altered metarhyolite.|c. 1880 Ma|||Intruded by the Woodward Dolerite.|Mafic volcanic rocks interbedded with minor felsic volcanic rocks, and siliciclastic and calcareous metasedimentary rocks.|
1737|Biscay Formation|73089|5|Briefly described|p25-27, p32-33, p37|Orosirian|Orosirian|Lamboo Province, Eastern Zone. Possibly broadly correlative to Dead Bullock and Stubbins formations. Dominantly Paleoproterozoic detritus. [Unclear whether the following intrude the unit or are considered part of it]. Contains basalts of similar age to those of the Tickalara Metamorphics. Basalts have characteristics similar to those emplaced in continental passive margins.|c. 1875-1855 Ma|||Unconformably underlain by Brim Rockhole Formation. Overlain by Olympio Formation.|Metasedimentary rocks including basalt[?].|
1809|Black Range Dolerite|23575|5|Briefly described|Map Legend|||Geological Province: Hamersley Basin..||||||26-JUL-07
1809|Black Range Dolerite|37818|6|Mentioned|p78|||||||||
1809|Black Range Dolerite|38763|6|Mentioned|p108|||||||||
1809|Black Range Dolerite|72712|6|Mentioned|p10 Fig.7.|||Unconformably overlain by Hardey Formation. (discussion of Fig.7 on p8).|2770+/-4 Ma (p8)|||||
1854|Blackfella Rockhole Member|23621|4|Described|p35|Cambrian|Cambrian|See also page 9 table 1. Of Antrim Plateau Volcanics. Geological Province: Ord Basin. Max. thickness: 100 m.||||||
1854|Blackfella Rockhole Member|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Antrim Plateau Volcanics. Geological Province: Ord Basin.||||||
1854|Blackfella Rockhole Member|24122|5|Briefly described|p12|Cambrian|Cambrian|Of Antrim Plateau Volcanics.||||||
1854|Blackfella Rockhole Member|24297|5|Briefly described|p17|Middle Cambrian|Middle Cambrian|Of Antrim Plateau Volcanics. Geological Province: Wiso Basin.||||||
1854|Blackfella Rockhole Member|28255|3|Fully described|p89|Cambrian|Cambrian|Of the Antrim Plateau Volcanics. Agglomerate and basalt; minor sandstone and siltstone.  Disconformably overlain by Headleys Limestone. Thickness at type section: 71m. See also Tb. 9 (before p83) p142 Appendix.||||||07-JUN-05
1854|Blackfella Rockhole Member|32172|4|Described|p10|||Table 2. L.Cambrian||||||
1854|Blackfella Rockhole Member|32173|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics.  Interbedded basalt and agglomerate, minor intercalated sandstone and siltstone beds.||||||16-NOV-04
1854|Blackfella Rockhole Member|33375|6|Mentioned|p10 Tb. 1,|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics. Agglomerate; vesicular basalt fragments 1-60cm set in altered basalt matrix. Overlain by Headleys Limestone. Max. thickness: ~60m.||||||27-APR-05
1854|Blackfella Rockhole Member|33378|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics. Agglomerate, brecciated flow tops.||||||27-APR-05
1854|Blackfella Rockhole Member|40993|6|Mentioned|Fig.1|||||||||
1854|Blackfella Rockhole Member|41840|1|Redefined|p40|Early Cambrian||||||||
1854|Blackfella Rockhole Member|41864|5|Briefly described|p12|||||||||
1854|Blackfella Rockhole Member|41865|6|Mentioned|Map Legend|Early Cambrian||||||||
1854|Blackfella Rockhole Member|41866|5|Briefly described|Map legend|Early Cambrian||||||||
1854|Blackfella Rockhole Member|43299|6|Mentioned|Map Legend||Cambrian|Of Antrim Plateau Volcanics.||||||25-JUL-06
1854|Blackfella Rockhole Member|43855|5|Briefly described|Map Legend||Early Cambrian|||||||
1854|Blackfella Rockhole Member|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
1854|Blackfella Rockhole Member|48943|2|Defined|p99|Early Cambrian|Early Cambrian|Strat. section p138.||||||25-JUL-06
1854|Blackfella Rockhole Member|60519|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics. Geological Province: Ord Basin. Fine grained basalt and basaltic breccia. Geological Province: Ord Basin.||||||03-NOV-04
1854|Blackfella Rockhole Member|60682|5|Briefly described|p21|Early Cambrian|Early Cambrian|Of the Antrim Plateau Volcanics.||||||
1854|Blackfella Rockhole Member|60685|5|Briefly described|p17|Cambrian|Cambrian|Of the Antrim Plateau Volcanics. Consists of agglomerate and minor sedimentary rocks.||||||
1854|Blackfella Rockhole Member|65337|6|Mentioned|p94.|||||Unit in Antrim Plateau Volcanics.||||
1854|Blackfella Rockhole Member|67151|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.||Unit in Antrim Plateau Volcanics.|||Agglomerate; brecciated flow tops.|
1854|Blackfella Rockhole Member|67860|4|Described|p420 Tb. 4-18, p421 fig 4-86|Early Cambrian|Early Cambrian|0-140 m thick. Type section details given.||Antrim Plateau Volcanics||Overlies Bingy Bingy Basalt Member conformably.|Fine-grained basalt and agglomerate.|
1854|Blackfella Rockhole Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Ord Basin||Antrim Plateau Volcanics|||Fine-grained basalt and basaltic breccia.|30-JUL-15
1854|Blackfella Rockhole Member|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||||||Fine grained basalt and basaltic breccia.|
1854|Blackfella Rockhole Member|69445|5|Briefly described|p30:3-4; 30:6 Fig.30.5; 30:16-17|Early Cambrian|Early Cambrian|Sweet et al. (1974). Southern Victoria River region.||Antrim Plateau Volcanics.|||Intercalating agglomerate (consisting of extensively altered angular to rounded fragments of vesicular and amygdaloidal basalt set in an aphanitic, heavily altered basaltic matrix); minor basaltic lavas; thin lenses of sandstone and siltstone.|12-JUL-16
1854|Blackfella Rockhole Member|69634|4|Described|100k_interpgeop_lut.csv|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny.|508-505 Ma (Inferred)|Unit of Antrim Plateau Volcanics.|||Fine-grained basalt and basaltic breccia|
1854|Blackfella Rockhole Member|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||505-508 Ma|Antrim Plateau Volcanics|||Fine grained basalt and basaltic breccia.|
1854|Blackfella Rockhole Member|70315|3|Fully described|p22-p24, p26-p35|||Kalkarindji Province. The type locality occurs at Blackfella Rockhole and was defined by Sweet et al (1974) [description of type locality provided]. 70-130m thick. Crops out as a broadly "horse-shoe" shapped patern fringing the Ord basin. Outcrop at various localities are described in some detail Referred to as the BRM throughout the text. Flow characteristics and description is provided.||Antrim Plateau Volcanics||Overlies the Bingy Bingy Basalt Member.|Laterally-extensive, thick volcanic breccia succession capped by a prominent overlying limestone.|
1854|Blackfella Rockhole Member|70655|5|Briefly described|Map Legend|Cambrian|Cambrian|Kalkarindji Province.||Antrim Plateau Volcanics.|||Agglomerate, brecciated flow tops.|
1854|Blackfella Rockhole Member|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|508-505 Ma|Unit of Antrim Plateau Volcanics.|||Interbedded basalt and agglomerate, minor intercalated sandstone and siltstone|
1959|Blinker Hill Sandstone Member|23722|5|Briefly described|p20|||Parent: Warton Sandstone.   Geological Province: Kimberley Basin||||||
1959|Blinker Hill Sandstone Member|30897|6|Mentioned|p13|||Stratigraphy||||||
1959|Blinker Hill Sandstone Member|36551|6|Mentioned|p33|||||||||
1959|Blinker Hill Sandstone Member|42814|6|Mentioned|p14|||of Warton Sandstone on Koolan Island||||||
1988|Blue Hills Sandstone|22746|6|Mentioned|Fig.3 p515|Ordovician|Ordovician|||||||
1988|Blue Hills Sandstone|22922|6|Mentioned|34|||||||||
1988|Blue Hills Sandstone|23282|2|Defined|p83|Early Silurian|Late Ordovician|Informally used as 'Policeman Well Sandstone' by Packham & Webby (1969). Krieg (1973) introduced Blue Hills Sandstone. The overlying 'Cartu beds' & 'Mintabie beds' are taken as synonyms. Age: Late Ordovician to Early Silurian 445-435Ma. of Munda Group.||||||
1988|Blue Hills Sandstone|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
1988|Blue Hills Sandstone|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|||||||
1988|Blue Hills Sandstone|23858|5|Briefly described|p917|Ordovician|Cambrian|Overlying Unit Mimili Formation. Geological Province: Officer Basin. Max. thickness: 800 m.||||||
1988|Blue Hills Sandstone|24067|5|Briefly described|p249|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
1988|Blue Hills Sandstone|24112|5|Briefly described|p254 Fig.2|Early Silurian|Late Ordovician|Of the Munda Group. Geological Province: Officer Basin||||||
1988|Blue Hills Sandstone|30544|6|Mentioned|p47|||||||||
1988|Blue Hills Sandstone|30807|6|Mentioned|p102|||Suggested map symbol.||||||
1988|Blue Hills Sandstone|30921|6|Mentioned|Map legend|Ordovician|Ordovician|Cambro-Ordovician.||||||
1988|Blue Hills Sandstone|30923|6|Mentioned|Map legend|Cambrian|Cambrian|Cambro-Ordovician||||||
1988|Blue Hills Sandstone|31457|6|Mentioned|p13|||||||||
1988|Blue Hills Sandstone|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
1988|Blue Hills Sandstone|33738|6|Mentioned|p58|||||||||
1988|Blue Hills Sandstone|35628|4|Described|Table 3|||||||||
1988|Blue Hills Sandstone|36096|6|Mentioned|Fig.3|||||||||
1988|Blue Hills Sandstone|36491|6|Mentioned|Fig.2|||||||||
1988|Blue Hills Sandstone|36895|6|Mentioned|p9|||||||||
1988|Blue Hills Sandstone|36920|6|Mentioned|Table 1|||||||||
1988|Blue Hills Sandstone|38022|6|Mentioned|Fig.4|||||||||
1988|Blue Hills Sandstone|38329|6|Mentioned|p194|||||||||
1988|Blue Hills Sandstone|40003|5|Briefly described|Table 15|||||||||
1988|Blue Hills Sandstone|40136|5|Briefly described|p18|||||||||
1988|Blue Hills Sandstone|40926|6|Mentioned|p12|||||||||
1988|Blue Hills Sandstone|42346|5|Briefly described|Fig.4 P82|Middle Ordovician||||||||
1988|Blue Hills Sandstone|43052|5|Briefly described|Fig.2.10|||||||||
1988|Blue Hills Sandstone|43085|5|Briefly described|Fig.7|||||||||
1988|Blue Hills Sandstone|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
1988|Blue Hills Sandstone|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
1988|Blue Hills Sandstone|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
1988|Blue Hills Sandstone|43743|6|Mentioned|Fig.2,p33|Early Silurian|Late Ordovician|||||||
1988|Blue Hills Sandstone|44109|5|Briefly described|p22 Fig. 25|Ordovician|Ordovician|Geological Province: central Officer Basin.||||||
1988|Blue Hills Sandstone|44133|5|Briefly described|p40-41, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Overlies conformably the Indulkana Shale. ||||||07-NOV-08
1988|Blue Hills Sandstone|45149|6|Mentioned|p43|||See also Table 1 and P15.||||||
1988|Blue Hills Sandstone|49792|5|Briefly described|Fig.5|||||||||
1988|Blue Hills Sandstone|65313|6|Mentioned|p580 Fig. 8|Silurian|Silurian|Officer Basin.||Munda Group.||Overlies Indulkana Shale.||26-MAR-12
1988|Blue Hills Sandstone|71146|5|Briefly described|p6|Llandovery|Late Ordovician|Officer Basin.||Munda Group||Overlies the Indulkana Shale and the Mount Chandler Sandstone. Unconformably overlain by the Mimili Formation.|Sandstone.|
1988|Blue Hills Sandstone|72478|6|Mentioned|p8|Early Silurian|Late Ordovician|Officer Basin.|c. 445-437 Ma|Munda Group||Overlies the Indulkana Shale. Unconformably underlies the Mimili Formation and the Boorthanna Formation.||
1988|Blue Hills Sandstone|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Sandstone, red-brown, fine- to medium-grained, kaolinitic, with pebble beds; trace fossils, cross-bedded.|
1988|Blue Hills Sandstone|73235|6|Mentioned|p60|||||||||
2050|Bobbies Point Alkali Granite|40811|4|Described|p320|||||||||
2050|Bobbies Point Alkali Granite|43715|6|Mentioned|p27|||||||||
2055|Bobs Bore Conglomerate|22741|5|Briefly described|P21, P23, Table3 P16||Devonian|||||||
2055|Bobs Bore Conglomerate|24061|6|Mentioned|p175|||Geological Province:  Canning Basin.||||||
2055|Bobs Bore Conglomerate|31332|6|Mentioned|Fig. 3|||Frasnian||||||
2055|Bobs Bore Conglomerate|33042|6|Mentioned|p725|||||||||
2055|Bobs Bore Conglomerate|36225|6|Mentioned|Map legend|Famennian|Frasnian|Frasnian to Famennian||||||
2055|Bobs Bore Conglomerate|36890|3|Fully described|p335|||||||||
2055|Bobs Bore Conglomerate|42030|6|Mentioned|p748|||||||||
2055|Bobs Bore Conglomerate|43666|6|Mentioned|p22|||||||||
2055|Bobs Bore Conglomerate|44397|14|Not recorded|p.12, Fig.3, Table 4|||Famennian (?) to Frasnian.||||||
2055|Bobs Bore Conglomerate|44398|14|Not recorded|map legend|||Fammenian? to Frasnian.||||||
2055|Bobs Bore Conglomerate|45101|6|Mentioned|Fig.8|||||||||
2055|Bobs Bore Conglomerate|64580|6|Mentioned|map legend|||Frasnian and Famennian conglomerates associated with Devonian reef complexes.||||||15-DEC-08
2055|Bobs Bore Conglomerate|66127|4|Described|p133 Fig.187, p134, p287, Plates 4, 7.|Early Famennian|Middle Frasnian|Southern Lennard Shelf. Type section is in the Virgin Hills, from 5 km W to 7 km WNW of Bobs Bore. Poorly exposed; 200 to 400 m thick. Clasts, mainly quartzite, from the Kimberley Basin. |c. 381 - 374 Ma.|||Interbedded with Virgin Hills Formation.|Siliciclastic cobble to boulder conglomerate and  coarse-grained conglomeratic sandstone; deep-water submarine-fan deposits.|
2055|Bobs Bore Conglomerate|69099|5|Briefly described|500k_geologyp08_lut.csv|Famennian|Frasnian|Frasnian and Famennian conglomerates associated with Devonian reef complexes|||||Conglomerate and sandstone.|30-JUL-15
2055|Bobs Bore Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Frasnian|||||||
2055|Bobs Bore Conglomerate|71267|6|Mentioned|1M_geologyp12_lut.csv||||||||Boulder, cobble and pebble conglomerate, sandstone, clasts mainly of Precambrian quartzite|
2126|Boll Conglomerate|22537|6|Mentioned|42|||Parent Mahoney Group||||||
2126|Boll Conglomerate|23858|5|Briefly described|p919|||Of Mahony Group. Geological Province: Ord Basin.||||||
2126|Boll Conglomerate|41598|6|Mentioned|p412|||||||||
2126|Boll Conglomerate|41811|6|Mentioned|p210|||||||||
2126|Boll Conglomerate|41840|2|Defined|p44|Devonian?||||||||
2126|Boll Conglomerate|41864|3|Fully described|p57|||||||||
2126|Boll Conglomerate|41865|5|Briefly described|Map legend||Frasnian|||||||
2126|Boll Conglomerate|41866|5|Briefly described|Map legend|Frasnian||||||||
2126|Boll Conglomerate|42030|4|Described|p750|||||||||
2126|Boll Conglomerate|43855|5|Briefly described|Map Legend||Frasnian|||||||
2126|Boll Conglomerate|44868|5|Briefly described|Map Legend||Frasnian|||||||
2126|Boll Conglomerate|64580|6|Mentioned|map legend|||Of Mahony Group.||||||15-DEC-08
2126|Boll Conglomerate|65417|5|Briefly described|p165.|Frasnian|Frasnian|Hardman Sub-basin. Upward-coarsening alluvial-fan deposits from uplift of the Osmand Range to the north.||||||
2126|Boll Conglomerate|67860|4|Described|p418 Tb. 4-18; p422,424 Figs. 4-88,4-90|Frasnian|Frasnian|Occurs as a lens high within Glass Hill Sandstone. Type section details given. Alluvial fan deposit. 0-350 m thick. Also appears as Boll Creek Conglomerate in Tb.4-18. Restricted to NW Bungle Bungle Range.||Mahony Group|||Conglomerate, pebbly sandstone, sandstone, rare siltstone.|19-JAN-17
2126|Boll Conglomerate|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Frasnian|Frasnian|||Mahony Group||||
2126|Boll Conglomerate|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Ord Basin||Mahony Group|||Redbed conglomerate, sandstone (commonly pebbly); rare siltstone.|30-JUL-15
2126|Boll Conglomerate|69165|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|||Mahony Group|||Redbed conglomerate, sandstone (commonly pebbly); rare siltstone.|
2126|Boll Conglomerate|69634|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny.|382.7-372.2 Ma (Biostrat)|Unit of Mahony Group.|||Redbed conglomerate, sandstone (commonly pebbly); rare siltstone|
2126|Boll Conglomerate|70154|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian||372-383 Ma|Mahony Group|||Redbed conglomerate, sandstone (commonly pebbly); rare siltstone.|
2126|Boll Conglomerate|71146|5|Briefly described|p6|Frasnian|Givetian|Ord Basin.||Mahony Group|||Sandstone and conglomerate.|
2126|Boll Conglomerate|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|382.7-372.2 Ma (biostrat)|Unit of Mahony Group.|||Pebble to boulder conglomerate pebbly sandstone, quartz arenite and minor siltstone|
2126|Boll Conglomerate|73255|6|Mentioned|p534 Fig.2|Devonian|Devonian|||Mahony Group||Overlies the Glass Hill Sandstone||
2153|Bon Accord Jaspilite Member|30562|4|Described|p38|||See also P9. Of Noganyer Formation.||||||27-NOV-09
2153|Bon Accord Jaspilite Member|43162|6|Mentioned|6|||||||||
2161|Bonaparte Formation|7142|6|Mentioned|p350 Fig.4.|Early Carboniferous|Late Devonian|Browse Basin.||||Is overlain by Milligans Formation.||
2161|Bonaparte Formation|12733|6|Mentioned|p565.|||Bonaparte Basin. May contain oil-prone facies.||||||
2161|Bonaparte Formation|13194|6|Mentioned|p382, p390, p391, p402.|Late Tournaisian|Late Devonian|See Table 4-16 and Figures 4-59 and 4-66. Type Section: Bonaparte 1 well (2280-3210m). 279-930m thick marine, offshore deposits. Only known from petroleum exporation wells.||Langfield Group||Laterally equivalent to Langfield Group, Ningbing Group, Cockatoo Group.  Probably Overlies Carlton Group.|Shale, siltstone, sandstone; minor sandy limestone.|
2161|Bonaparte Formation|13234|5|Briefly described|p250 Fig.2 ,p251-252, p260 Tb.1, |Early Carboniferous|Late Devonian|Clay-rich basinal facies. Proven reservoir. Potential seal. Gas flows.||||||
2161|Bonaparte Formation|13354|6|Mentioned|p375 Fig.6.|Early Carboniferous|Devonian|Underlies Milligans Formation.||31||||28-OCT-14
2161|Bonaparte Formation|14228|6|Mentioned|p6 fig3|Tournaisian|Givetian|Southern Bonaparte Basin. [Database has Bonaparte Formation being purely Tournaisian]||||||
2161|Bonaparte Formation|23377|6|Mentioned|p212 Fig.5|Carboniferous|Devonian|Of Vulcan Sub-basin.||||||26-JUL-06
2161|Bonaparte Formation|24246|5|Briefly described|p7|||Geological Province: Bonaparte Basin.||||||
2161|Bonaparte Formation|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin.||||||
2161|Bonaparte Formation|24569|5|Briefly described|p248 Fig. 3|Tournaisian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
2161|Bonaparte Formation|40792|6|Mentioned|Fig.3|||||||||
2161|Bonaparte Formation|40993|2|Defined|p10|Tournaisian|Late Devonian|Late Devonian to Tournaisian.||||||11-APR-08
2161|Bonaparte Formation|41532|4|Described|p292|||||||||
2161|Bonaparte Formation|41839|4|Described|p32|||Formerly "Bonaparte Beds".||||||11-APR-08
2161|Bonaparte Formation|41864|3|Fully described|p122|||||||||
2161|Bonaparte Formation|41865|5|Briefly described|Map legend|Tournaisian|Middle Devonian|||||||
2161|Bonaparte Formation|42030|5|Briefly described|p748|||||||||
2161|Bonaparte Formation|42055|4|Described|Fig.1 P52|||||||||
2161|Bonaparte Formation|42056|4|Described|p96|||||||||
2161|Bonaparte Formation|42442|3|Fully described|p11|||Age Late Devonian to Early Carboniferous (late Tournaisian).||||||11-APR-08
2161|Bonaparte Formation|42547|4|Described|p101, p104|||||||||
2161|Bonaparte Formation|42564|6|Mentioned|p47|||||||||
2161|Bonaparte Formation|43482|6|Mentioned|23||Late Devonian|||||||
2161|Bonaparte Formation|50085|5|Briefly described|p2 Fig. 2, p3 Tb. 1||Devonian|Geological Province: Bonaparte Basin.||||||
2161|Bonaparte Formation|60364|4|Described|p190|Late Devonian|Late Devonian|Offshore shale and siltstone equivalent of Langfield and Ningbing Groups. Unconformably overlain by Milligans Formation. Geological Province: Bonaparte Basin.||||||
2161|Bonaparte Formation|60386|6|Mentioned|p297|Carboniferous||Roebuck/Canning Basin. Pre-Alice Springs Orogeny.||||||
2161|Bonaparte Formation|60682|4|Described|p22 Table 5, 24|Tournaisian|Tournaisian|Of Langfield Group. Max. thickness: >279m. Shale, siltstone, dolomitic sandstone and quartzitic limestone. Possibly laterally equivalent to Cockatoo, Langfield and Ninbing Groups. Geological Province: Bonaparte Basin.||||||
2161|Bonaparte Formation|61023|5|Briefly described|p2 Fig. 2|Devonian|Devonian|Geological Province: Bonaparte Basin.||||||11-APR-08
2161|Bonaparte Formation|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
2161|Bonaparte Formation|62837|5|Briefly described|Stratigraphic columns|Visean|Tournaisian|Of the Langfield Group.  Age:355->345Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
2161|Bonaparte Formation|64580|6|Mentioned|map legend|||Of Langfield Group.||||||15-DEC-08
2161|Bonaparte Formation|64694|5|Briefly described|p234 Fig.2, p235, p236, p238 Tb.1|Tournaisian|Famennian|Divided into a lower and an upper part on the basis of different palynological Assemblages (Retispora lepidophyta and Grandispora spiculifera respectively).||||Is overlain unconformably by Tanmurra Formation and Milligans Formation.||
2161|Bonaparte Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes grey fine- to medium-grained sandstone.|22-DEC-22
2161|Bonaparte Formation|67200|5|Briefly described|app 2 p8||||||||Fine to medium grained sandstone.|
2161|Bonaparte Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournasian|Tournasian|||Langfield Group||||
2161|Bonaparte Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||
2161|Bonaparte Formation|69452|3|Fully described|p36:6-7, 9, 12, 15|Carboniferous|Late Devonian|Beere and Mory (1986). Equivalent to the Bonaparte beds of Veevers and Roberts (1968). Bonaparte Basin. Only known from onshore petroleum exploration wells in CAMBRIDGE GULF map area in WA. Possibly occurs in subsurface northwestern NT and in offshore Petrel Sub-basin. Quiet relatively deep-marine deposits. Type section is the interval 2280-3210m in drillhole Bonaparte-1, although the Formation's base was not reached: over 930m thick. Onshore and probably offshore. Long-ranging unit is also a lateral equivalent of Cockatoo Group and other Langfield Group units.||Langfield Group.||Partly laterally equivalent to, and overlies conformably and disconformably, Ningbing Group.|Shale, siltstone with interbedded variably dolomitic sandstone and minor quartzose limestone.|12-JUL-16
2161|Bonaparte Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Unit of Langfield Group.||||
2161|Bonaparte Formation|69653|6|Mentioned|p10|Carboniferous|Devonian|Petrel Sub-basin.||||Is overlain by Milligans Formation (Weaber Group). Equivalent to Cockatoo, Ningbing and Langfield Groups.||
2161|Bonaparte Formation|69673|4|Described|p168 fig 139, p171 fig 142, p171, p177|Carboniferous|Devonian|Deposited in quiet water marine shelf or deep basin settings.||Langfield Group|||Shale and siltstone with interbedded variably dolomitic sandstone and minor quartzose limestone.|
2161|Bonaparte Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.3, p2-3|Tournaisian|Frasnian|See also Regional geology: Fig.8, p9, p11. Includes hydrocarbon source rocks (Langfield Group equivalent) and reservoir rocks, as well as regional and intraformational (Langfield and Ningbing Groups equivalent) seals. Shale facies may provide additional unconventional resource potential.||||Is overlain by Milligans Formation.|Includes anoxic marine mudstones.|12-JUL-16
2161|Bonaparte Formation|71146|5|Briefly described|p6,  p43 fig 33|Tournaisian|Eifelian|Bonaparte Basin.||||Unconformably overlain by the Weaber Group.|Mudstone.|
2189|Boobina Porphyry|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3305 Ma||||||07-NOV-08
2189|Boobina Porphyry|23255|5|Briefly described|p50||Archean|Age: U-Pb 3307 +/- 19 Ma. of Corunna Downs Batholith.||||||16-APR-13
2189|Boobina Porphyry|31853|2|Defined|p61|Archean|Archean|||||||07-NOV-08
2189|Boobina Porphyry|35641|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
2189|Boobina Porphyry|36551|6|Mentioned|p75|||||||||
2189|Boobina Porphyry|38507|6|Mentioned|Fig.1|||||||||
2189|Boobina Porphyry|39444|4|Described|p40|||||||||
2189|Boobina Porphyry|39580|4|Described|p293|||||||||
2189|Boobina Porphyry|39672|5|Briefly described|p238|||||||||
2189|Boobina Porphyry|39697|6|Mentioned|p78|||||||||
2189|Boobina Porphyry|40596|6|Mentioned|p65|||||||||
2189|Boobina Porphyry|41250|6|Mentioned|p31|||||||||
2189|Boobina Porphyry|41349|6|Mentioned|p4|||||||||
2189|Boobina Porphyry|50381|5|Briefly described|Map Legend|Archean|Archean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Age: c. 3315 Ma||||||07-NOV-08
2189|Boobina Porphyry|63417|5|Briefly described|Map legend|Archean|Archean|Of Emu Pool Supersuite.  Age: 3315 Ma. Geological Province: Pilbara Craton. Quartz-feldspar porphyry; minor hornblende; metamorphosed.||||||16-APR-13
2189|Boobina Porphyry|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Ages: 3315 +/- 4 Ma and 3307 +/- 19 Ma. Geological Province: Pilbara Craton.||||||16-APR-13
2189|Boobina Porphyry|64327|4|Described|p62, p63 Fig. 2, p64|Archean|Archean|Of Corunna Downs Granitoid Complex. Age: 3315 Ma (SHRIMP). Intruded the Warrawoona Group. Hornblende-bearing, quartz-feldspar porphyry with a glassy pink to purple matrix. Hosts a number of copper-mineralised quartz veins.||||||16-APR-13
2189|Boobina Porphyry|64328|5|Briefly described|p55 Fig. 1, p57|Archean|Archean|Age: 3315 +/- 4 Ma. Intruded the Euro Basalt.  See also p57 Tb. 2.||||||16-APR-13
2189|Boobina Porphyry|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Corunna Downs Granitoid Complex. Geological Province: Pilbara Craton. Quartz-feldspar porphyry; minor hornblende; metamorphosed.||||||07-FEB-11
2189|Boobina Porphyry|65008|4|Described|p11, p12, p41|Paleoarchean|Paleoarchean|Geochronology includes a U-Pb zircon age of 3307 +/- 19 Ma (Pidgeon, 1984) and a U-Pb zircon SHRIMP date of 3315 +/- 4 Ma (Barley and Pickard, 1999).|3307 +/- 19 Ma; 3315 +/- 4 Ma|Of the Corunna Downs Granitoid Complex||Intrudes the Wyman Formation and the Euro Basalt. Intruded by the Mondana Monzogranite.|Quartz-feldspar porphyry; minor hornblende; metamorphosed.|
2189|Boobina Porphyry|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Emu Pool Supersuite. c.3315 Ma. Porphyritic fine-grained monzogranite; minor hornblende; weakly metamorphosed.||||||
2189|Boobina Porphyry|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3321-3307 Ma|Of the Emu Pool Supersuite.|||Comprises porphyritic fine-grained monzogranite; minor hornblende; weakly metamorphosed.|
2189|Boobina Porphyry|69041|4|Described|p11, p13|Paleoarchean|Paleoarchean|Pilbara Craton. Occurs as enclaves within the Mondana Suite. Crops out along the southeast argin of the Corruna Downs Igneous Complex. Defined and first described by Lipple (1975). A SHRIMP age of 3315 +/- 2 Ma is derived from Barley and Pickard (1999). Accessory minerals are described.|3307 +/- 19 Ma (Pidgeon, 1984)||||Dark feldspar-quartz-biotite porphyry consisting of euhedral to subhedral oligoclase and subordinate quartz in a dark aphanitic groundmass.|
2189|Boobina Porphyry|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean||||||Porphyritic fine-grained monzogranite; minor hornblende; weakly metamorphosed. Sericite-altered, porphyritic, fine-grained metamonzogranite.|
2189|Boobina Porphyry|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|3321-3307 Ma (isotopic; inferred)|Unit of Emu Pool Supersuite.|||Porphyritic fine-grained monzogranite; minor hornblende; weakly metamorphosed|
2189|Boobina Porphyry|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||porphyry|
2189|Boobina Porphyry|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean||Max age 3324+/-4 Ma, min 3307+/-19 Ma.|Emu Pool Supersuite|||Porphyritic fine-grained monzogranite; minor hornblende; weakly metamorphosed.|
2196|Bookara Sandstone Member|23279|5|Briefly described|p20-1||Early Triassic|(Playford et al., 1976).||||||
2196|Bookara Sandstone Member|23520|5|Briefly described|p11 Fig. 7|Early Triassic|Early Triassic|Of the Kockatea Shale. Geological Province: Perth Basin. See also p9.||||||21-APR-08
2196|Bookara Sandstone Member|29693|6|Mentioned|Fig.7|||||||||
2196|Bookara Sandstone Member|31910|4|Described|Table 1|||||||||
2196|Bookara Sandstone Member|36293|6|Mentioned|p123|||See also P260.||||||
2196|Bookara Sandstone Member|41195|6|Mentioned|p322|||||||||
2196|Bookara Sandstone Member|43495|5|Briefly described|9||Scythian|||||||
2196|Bookara Sandstone Member|44144|6|Mentioned|p507 Tb.4-21, p513 Fig.4-152|Early Triassic|Early Triassic|Shoreline deposit.||Kockatea Shale||||
2196|Bookara Sandstone Member|60377|5|Briefly described|p61 Fig. 3. |Scythian|Wuchiapingian|Of the Kockatea Shale. Sandstone and Member in the text are Sst and Mbr respectively. Geological Province: Perth Basin. Marin depositional environment.||||||07-FEB-11
2196|Bookara Sandstone Member|61811|5|Briefly described|p3 Fig.2, p35, p62.|Early Triassic|Late Permian|Northern Perth Basin. Type section details in Appendix 1.||Unit in Kockatea Shale.||||
2196|Bookara Sandstone Member|64635|5|Briefly described|p4 Fig.3, p7  |Induan|Induan|||Unit in Kockatea Shale.||||
2196|Bookara Sandstone Member|67340|6|Mentioned|p6|Permian|Permian|Northern Perth Basin.||Kockatea Shale.||||
2196|Bookara Sandstone Member|69182|6|Mentioned|Ch2 p34-p41|||||||||
2216|Boolaloo Granodiorite|22512|4|Described|P284||Statherian|Age of unit is 1786+/-5 Ma||||||
2216|Boolaloo Granodiorite|23570|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton||||||07-NOV-08
2216|Boolaloo Granodiorite|23612|5|Briefly described|p839|||Geological Province: Hamersley Basin.||||||
2216|Boolaloo Granodiorite|23774|5|Briefly described|p733 table 1|||Age: 1786+/-5 Ma. Also see Boolaloo Granite.||||||
2216|Boolaloo Granodiorite|24183|5|Briefly described|p6|Statherian|Statherian|Age: 1786 +/- 5 Ma.||||||
2216|Boolaloo Granodiorite|24197|6|Mentioned|p71 Tb. 7.1|||Of the Boolaloo Supersuite.||||||07-FEB-11
2216|Boolaloo Granodiorite|24544|6|Mentioned|p45|||||||||
2216|Boolaloo Granodiorite|24602|5|Briefly described|p855 Fig.2|||Of the Wyloo Group. Age: 1786 +/- 5 Ma (SHRMIP U-Pb zircon, Kapez and McNaughton, 1999) & ca. 1680 (Rb-Sr, Leggo at al, 1965). Geological Province: Ashburton Fold Belt. See also p861.||||||
2216|Boolaloo Granodiorite|24607|5|Briefly described|p968, 970|Paleoproterozoic|Paleoproterozoic|Age: 1786 +/- 5 Ma. Intrudes Ashburton Formation. Geological Province: Ashburton Basin.||||||30-NOV-10
2216|Boolaloo Granodiorite|29845|6|Mentioned|p171|||||||||
2216|Boolaloo Granodiorite|30488|6|Mentioned|p89|||||||||
2216|Boolaloo Granodiorite|33542|6|Mentioned|p412|||||||||
2216|Boolaloo Granodiorite|33543|6|Mentioned|p134|||||||||
2216|Boolaloo Granodiorite|34066|6|Mentioned|p13|||Prot.||||||
2216|Boolaloo Granodiorite|35260|6|Mentioned|Fig.12|||||||||
2216|Boolaloo Granodiorite|35269|6|Mentioned|p315|||||||||
2216|Boolaloo Granodiorite|37327|6|Mentioned|p391|||||||||
2216|Boolaloo Granodiorite|37460|6|Mentioned|p127|||||||||
2216|Boolaloo Granodiorite|38321|6|Mentioned|Table 1|||||||||
2216|Boolaloo Granodiorite|40103|6|Mentioned|p197|||||||||
2216|Boolaloo Granodiorite|41846|6|Mentioned|p94|||||||||
2216|Boolaloo Granodiorite|41955|6|Mentioned|Fig.1 P4|||||||||
2216|Boolaloo Granodiorite|42260|6|Mentioned|p9|||||||||
2216|Boolaloo Granodiorite|42277|6|Mentioned|Fig.1 P56|||||||||
2216|Boolaloo Granodiorite|42435|6|Mentioned|Fig.1 P43|||||||||
2216|Boolaloo Granodiorite|43037|5|Briefly described|p25|||Of Wyloo Group[??]||||||18-JAN-07
2216|Boolaloo Granodiorite|50225|5|Briefly described|p388|Paleoproterozoic|Paleoproterozoic|Intrudes the upper Wyloo Goup.  Age: c.1786Ma.||||||07-FEB-11
2216|Boolaloo Granodiorite|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Intrudes the Wyloo Group.  Age: 1.78Ga (U-Pb zircon, Krapez and McNaughton, 1999).||||||07-NOV-08
2216|Boolaloo Granodiorite|50425|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province.  Of the Boolaloo Supersuite. Age: 1684Ma (Rb-Sr).||||||07-NOV-08
2216|Boolaloo Granodiorite|61262|6|Mentioned|p446 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: ~1780Ma. Geological Province: Ashburton Basin.||||||07-NOV-08
2216|Boolaloo Granodiorite|63866|4|Described|p154, p162, p177|Statherian|Statherian|SHRIMP age derived from Krapez and McNaughton, 1999.|1786 +/- 5 Ma (SHRIMP U-Pb zircon)|||Intrudes the Ashburton Formation.||
2216|Boolaloo Granodiorite|63869|5|Briefly described|p6, p14, p15, p27|Statherian|Statherian|SHRIMP U-Pb age.|1786 +/- 5 Ma (Krapez and McNaughton, 1999).|||Intrudes Ashburton Formation.||
2216|Boolaloo Granodiorite|65830|5|Briefly described|p3, p4|Statherian|Statherian||1786+/-5Ma SHRIMP U-Pb Krapez and McNaughton 1999|||Intrudes the Ashburton Formation.||
2216|Boolaloo Granodiorite|66299|6|Mentioned|pp202-203.|Paleoproterozoic|Paleoproterozoic||1786 +/- 5 Ma.|||||
2216|Boolaloo Granodiorite|66950|6|Mentioned|p15|||||||Cross-cuts the Ashburton Formation.||
2216|Boolaloo Granodiorite|67056|6|Mentioned|p419 Fig.2. |Paleoproterozoic|Paleoproterozoic||1786 Ma. |||||
2216|Boolaloo Granodiorite|67827|6|Mentioned|p427|||||||||
2216|Boolaloo Granodiorite|67855|5|Briefly described|p210, p211 fig 3-9, p220|Paleoproterozoic|Paleoproterozoic|Spelt Boolaloo Ganodiorite p220.|1680 Ma Rb-Sr (Leggo et al 1965).|||Intrudes Ashburton Formation, Wyloo Group.||
2216|Boolaloo Granodiorite|69003|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Crosscuts deformation in upper Wyloo Group, thereby constraining age of deformation.|1786 +/- 5 Ma.|||Intrudes upper Wyloo Group.||
2216|Boolaloo Granodiorite|69538|5|Briefly described|p517 Fig.3|Paleoproterozoic|Paleoproterozoic||1786 Ma.|||||
2216|Boolaloo Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
2216|Boolaloo Granodiorite|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Gascoyne Province.||Moorarie Supersuite.|||Fine- to medium-grained, seriate to strongly porphyritic biotite granodiorite; locally contains abundant mafic xenoliths.|
2216|Boolaloo Granodiorite|72712|6|Mentioned|p3.|||Included in the Hamersley province.|||||Includes granodiorite.|
2216|Boolaloo Granodiorite|72758|5|Briefly described|p10 Tb.1, p31, p41, p43, p46-48.|Statherian|Statherian|Rb/Sr mineral isochron age by Leggo and other (1965). Shows contact metamorphic aureole. See also p4 Fig.1.|c. 1684 Ma by Rb/Sr methods|||Intrudes Ashburton Formation, Morrisey Metamorphic Suite.|Granodiorite with abundant rounded mafic xenoliths, up to 0.3 m diameter.|
2216|Boolaloo Granodiorite|73214|5|Briefly described|p985|||Ashburton Basin.|1786 +/- 5 Ma (Krapez and McNaughton, 1999).|||||
2227|Boolgeeda Iron Formation|22689|6|Mentioned|Fig. 1 p138|||Of Hamersley Group.||||||
2227|Boolgeeda Iron Formation|22701|5|Briefly described|Fig2,p39|Paleoproterozoic|Neoarchean|Hamersley Group, Hamersley Basin. Overlies Woongara Volcanics.||||||07-NOV-08
2227|Boolgeeda Iron Formation|23046|6|Mentioned|177|||Overlying unit Turee Creek Group.||||||
2227|Boolgeeda Iron Formation|23047|5|Briefly described|38|||Of the Hamersley Group. Hamersley Province.  Max thickness 450 m. Underlain by Woongarra Rhyolite.||||||10-FEB-09
2227|Boolgeeda Iron Formation|23126|5|Briefly described|p383 Fig.3|||||||||
2227|Boolgeeda Iron Formation|23280|5|Briefly described|Fig2p1086|||||||||
2227|Boolgeeda Iron Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
2227|Boolgeeda Iron Formation|23570|5|Briefly described|p14|Archean|Archean|Of the Hamersley Group.    Geological Province: Pilbara Craton||||||07-NOV-08
2227|Boolgeeda Iron Formation|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Underlying unit Woongarra Rhyolite.||||||
2227|Boolgeeda Iron Formation|23612|5|Briefly described|p840|Archean|Archean|||||||07-NOV-08
2227|Boolgeeda Iron Formation|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Hamersley Group.  Age: c.2.47Ga.(U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||24-MAY-16
2227|Boolgeeda Iron Formation|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
2227|Boolgeeda Iron Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.47 Ga. Geological Province: Pilbara Craton. Underlain by Wongarra volcanics. Of the Hamersley Group.||||||01-MAR-10
2227|Boolgeeda Iron Formation|24231|5|Briefly described|p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
2227|Boolgeeda Iron Formation|24426|5|Briefly described|p218 Fig.3|Paleoproterozoic|Archean|Of Hamersley Group. Overlies Woongarra Volcanics. Geological Province: Hamersley Province.||||||07-FEB-11
2227|Boolgeeda Iron Formation|24544|4|Described|p47 Fig.35, p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Conformably overlies Woongarra Rhyolite. Conformably overlain by Kungarra Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
2227|Boolgeeda Iron Formation|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton||||||
2227|Boolgeeda Iron Formation|29716|4|Described|Table 1|||||||||
2227|Boolgeeda Iron Formation|30437|6|Mentioned|p98|||||||||
2227|Boolgeeda Iron Formation|31021|5|Briefly described|p893|||||||||
2227|Boolgeeda Iron Formation|31154|6|Mentioned|p71|||||||||
2227|Boolgeeda Iron Formation|31671|5|Briefly described|p12|||||||||
2227|Boolgeeda Iron Formation|31828|6|Mentioned|p32|||See also iron P41.||||||
2227|Boolgeeda Iron Formation|32326|6|Mentioned|p122|||Hamersley Gp.||||||
2227|Boolgeeda Iron Formation|33537|6|Mentioned|p110|||Analysis||||||
2227|Boolgeeda Iron Formation|33538|6|Mentioned|p291|||||||||
2227|Boolgeeda Iron Formation|33540|6|Mentioned|Fig.2|||||||||
2227|Boolgeeda Iron Formation|33542|6|Mentioned|p412|||||||||
2227|Boolgeeda Iron Formation|33543|5|Briefly described|p132|||||||||
2227|Boolgeeda Iron Formation|33544|2|Defined|p93|Proterozoic|Proterozoic|||||||
2227|Boolgeeda Iron Formation|34066|4|Described|p6|||L.Prot.||||||
2227|Boolgeeda Iron Formation|34135|4|Described|Table 1|||Lower Proterozoic. See also pp11,13,14.||||||06-OCT-15
2227|Boolgeeda Iron Formation|34887|6|Mentioned|p19|||||||||
2227|Boolgeeda Iron Formation|35218|6|Mentioned|Fig.1|||||||||
2227|Boolgeeda Iron Formation|35260|5|Briefly described|Table 3|||||||||
2227|Boolgeeda Iron Formation|35299|6|Mentioned|Fig.1|||||||||
2227|Boolgeeda Iron Formation|35976|6|Mentioned|p110|||See also Fig.39.||||||
2227|Boolgeeda Iron Formation|36247|6|Mentioned|Fig.2|||||||||
2227|Boolgeeda Iron Formation|36642|6|Mentioned|Table 1|||||||||
2227|Boolgeeda Iron Formation|36882|6|Mentioned|p135|||||||||
2227|Boolgeeda Iron Formation|37223|6|Mentioned|p10|||||||||
2227|Boolgeeda Iron Formation|37297|6|Mentioned|Fig.2|||||||||
2227|Boolgeeda Iron Formation|37460|6|Mentioned|Fig.3.4|||||||||
2227|Boolgeeda Iron Formation|37577|6|Mentioned|p30|||||||||
2227|Boolgeeda Iron Formation|37704|6|Mentioned|Fig.1|||||||||
2227|Boolgeeda Iron Formation|37708|6|Mentioned|Fig.1|||||||||
2227|Boolgeeda Iron Formation|38321|6|Mentioned|Table 1|||||||||
2227|Boolgeeda Iron Formation|38790|6|Mentioned|p163|||||||||
2227|Boolgeeda Iron Formation|39200|6|Mentioned|Fig.4|||||||||
2227|Boolgeeda Iron Formation|39210|5|Briefly described|Table 1|||||||||
2227|Boolgeeda Iron Formation|39589|6|Mentioned|p157|||||||||
2227|Boolgeeda Iron Formation|40369|6|Mentioned|Plate 1|||||||||
2227|Boolgeeda Iron Formation|41358|6|Mentioned|Fig.2|||||||||
2227|Boolgeeda Iron Formation|41768|5|Briefly described|Table 1|||See also P30 and P60||||||
2227|Boolgeeda Iron Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
2227|Boolgeeda Iron Formation|42148|6|Mentioned|p690|||||||||
2227|Boolgeeda Iron Formation|42190|6|Mentioned|p274|||||||||
2227|Boolgeeda Iron Formation|42471|4|Described|p8|||||||||
2227|Boolgeeda Iron Formation|42472|5|Briefly described|Map legend|||||||||
2227|Boolgeeda Iron Formation|42495|6|Mentioned|p35|||||||||
2227|Boolgeeda Iron Formation|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
2227|Boolgeeda Iron Formation|42704|5|Briefly described|Plate 2E|Proterozoic|Archean|Of the Hamersely Group. Fine-grained, flaggy iron formation, chert, jaspilite and shale.||||||07-NOV-08
2227|Boolgeeda Iron Formation|42743|5|Briefly described|map legend|Proterozoic||||||||
2227|Boolgeeda Iron Formation|42744|4|Described|p5|||||||||
2227|Boolgeeda Iron Formation|43119|4|Described|p11|||of Hamersley Group||||||
2227|Boolgeeda Iron Formation|43210|5|Briefly described|Table1 p3,p5.||Paleoproterozoic|of Hamersley Group||||||07-NOV-08
2227|Boolgeeda Iron Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Hamersley Group.||||||
2227|Boolgeeda Iron Formation|43290|4|Described|p7||Proterozoic|of Hamersley Group.||||||
2227|Boolgeeda Iron Formation|43595|6|Mentioned|Fig.2-49,p220|||||||||
2227|Boolgeeda Iron Formation|44152|5|Briefly described|p179 Fig.2-155, p182, p185 Tb.2-25, p187|||See also p188 Fig.2-161. Detailed comparison of this with similar BIF units of Hamersley Group on page 185.||Hamersley Group||Overlies Woongarra Volcanics. Is overlain by Turee Creek Group.|BIF, shale.|
2227|Boolgeeda Iron Formation|44438|14|Not recorded|map legend||Paleoproterozoic|Formation of Hamersley Group. L.Proterozoic.||||||07-NOV-08
2227|Boolgeeda Iron Formation|44477|4|Described|p.11, Table 1||Proterozoic|SF/50-6.||||||
2227|Boolgeeda Iron Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
2227|Boolgeeda Iron Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
2227|Boolgeeda Iron Formation|44501|4|Described|p.6,20,Table 4, map||Paleoproterozoic|Lower Proterozoic, (ref. to MacLeod et al 1963). (F50-7).||||||07-NOV-08
2227|Boolgeeda Iron Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
2227|Boolgeeda Iron Formation|44503|2|Defined|p.16,17,Tb.2, map|||See also p.8,20 for more details. Roy Hill Sheet. (F50-12).||||||
2227|Boolgeeda Iron Formation|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
2227|Boolgeeda Iron Formation|44692|2|Defined|p.7,11,16-19,23, map|||||||||
2227|Boolgeeda Iron Formation|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
2227|Boolgeeda Iron Formation|50227|6|Mentioned|p447 Fig. 3|||||||||07-FEB-11
2227|Boolgeeda Iron Formation|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersly Group. Overlian by Turee Creek Group, underlain by Woongarra Volcanics.||||||
2227|Boolgeeda Iron Formation|61265|5|Briefly described|p46-47 Fig.2|||Of the Hamersley Group. Geological Province: Pilbara Craton.||||||
2227|Boolgeeda Iron Formation|62129|3|Fully described|p11, p18|Archaean|Archaean|Of Hamersley Group. Conformably overlies Woongarra Rhyolite, overlian by Turee Creek Group. Thickness: 250m. Geological Province: Hamersley Basin. Comprises massive black to dark yellow-brown BIF, shale and purple-black, thinly bedded and fissile BIF.||||||07-FEB-11
2227|Boolgeeda Iron Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton. Fine-grained, finely laminated iron-formation, pelite and chert.||||||23-MAR-09
2227|Boolgeeda Iron Formation|63153|6|Mentioned|p1361 Fig.2, p1362 Fig.3.|||||Unit in Hamersley Group.||Overlies Woongarra Volcanics. Is overlain by Turee Creek Group.||
2227|Boolgeeda Iron Formation|63372|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Hamersley Basin. Fine-grained, finely laminated banded iron formation; mudstone, siltstone and chert. Overlies the Woongarra Rhyolite.||||||23-DEC-09
2227|Boolgeeda Iron Formation|63432|5|Briefly described|p736 Fig. 2|Proterozoic|Proterozoic|||||||07-FEB-11
2227|Boolgeeda Iron Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Upper Hamersley Group. Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies.||||||09-DEC-08
2227|Boolgeeda Iron Formation|64724|5|Briefly described|p42 Fig. 3|Paleoproterozoic|Paleoproterozoic|Hamersley Basin unit.||Of Hamersley Group.||||02-APR-12
2227|Boolgeeda Iron Formation|64830|4|Described|p1107-8|||Of Hamersley Gp (Mount Bruce Supergp). Overlies Woongarra Rhyolite. Geological province: Hamersley Basin (Ophthalmia Range). Hosts Hickman Crater at contact with Woongarra Rhyolite. Deformation of BIF resulted in megabbrecciation, shatter features,etc.||||||05-FEB-09
2227|Boolgeeda Iron Formation|65683|5|Briefly described|p801 Fig2|||Of Hamersley Group. Underlies Turee Creek Group; overlies Woongarra Volcanics.||||||08-MAR-12
2227|Boolgeeda Iron Formation|65757|5|Briefly described|p84 Fig.2|Siderian|Siderian|Age: 2445+/-5 Ma. Banded iron formation, overlies the Wongarra Rhyolite||||||
2227|Boolgeeda Iron Formation|66574|5|Briefly described|p912, p914 Fig.3|||In upper Hamersley Group. Deep marine and ferruginous siltstones; glacigenic diamictite contains clasts of Woongarra Rholite. Underlies Kungarra Formation, overlies Woongarra Rhyolite.||||||
2227|Boolgeeda Iron Formation|67025|4|Described|pp319-323.|||The natural remanent magnetisation and mean bulk susceptibility of this unit are discussed in this article.||Topmost unit in Hamersley Group.||Conformably overlies Woongarra Volcanics. Is overlain conformably by Turee Creek Group.|BIF, siltstone.|
2227|Boolgeeda Iron Formation|67056|5|Briefly described|p419 Fig.2. |||A possible source for a BIF jasper-rich type pebble conglomerate with occasional ore pebbles, which occurs in the Wyloo Group.||Unit in Hamersley Group.||||
2227|Boolgeeda Iron Formation|67130|5|Briefly described|p3 fig 2, p24 fig 17|||See also p31, p37, p38, p39 fig 36, p40 fig 37. ||Hamersley Group||Overlies Woongarra Rhyolite, overlain by Kungarra Formation|Banded iron formation, green shale|
2227|Boolgeeda Iron Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Hamersley Group||||
2227|Boolgeeda Iron Formation|67201|5|Briefly described|p34, p36, p53 Fig.40|||||Hamersley Group|||BIF-dominated.|
2227|Boolgeeda Iron Formation|67855|6|Mentioned|p225|||Hamersley Basin.||||||
2227|Boolgeeda Iron Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Of Hamersley Group.||Overlies Woongarra Rhyolite. Overlain by Kungarra Formation, Turee Creek Group.|BIF-dominated.|
2227|Boolgeeda Iron Formation|68280|6|Mentioned|p5, p41, p47, p48, p54, p57, p62|||||Hamersley Group||Overlain by Kungarra Formation, overlies Woongarra Rhyolite|Banded iron formation.|
2227|Boolgeeda Iron Formation|69003|6|Mentioned|p8||||||||BIF.|
2227|Boolgeeda Iron Formation|69028|5|Briefly described|Map Legend|Siderian|Siderian|Hamersley Basin.|2630-2445 Ma|Of the Hamersley Group.|||Fine-grained, finely laminated iron-formation, mudstone, siltstone and chert; metamorphosed.|07-MAY-14
2227|Boolgeeda Iron Formation|69080|6|Mentioned|p687|||||Topmost unit in Hamersley Group.||Overlies Weeli Wolli Formation.||
2227|Boolgeeda Iron Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies.|
2227|Boolgeeda Iron Formation|69185|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Hamersley Group.|||Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies|
2227|Boolgeeda Iron Formation|69538|6|Mentioned|p517 Fig.3|Paleoproterozoic|Paleoproterozoic|||Unit in Hamersley Group.||||
2227|Boolgeeda Iron Formation|69563|6|Mentioned|p691 Fig.1|||||Unit in Hamersley Group.||||
2227|Boolgeeda Iron Formation|69565|5|Briefly described|p131-132, p133 Fig.1, p134, 136-140|||Duck Creek Syncline, Hamersley Province. Previously, erroneously correlated with Meteorite Bore Member. Detrital pyrite sourced from underlying Fortescue and Hamersley Groups. Multiple S isotope data tabulated and discussed.||Hamersley Group.||Overlies Wongarra Rhyolite. Is overlain conformably by Kungarra Formation (Turee Creek Group).|Includes diamictites, sandstone, shale/mudstone. Pyrite grains (described in great detail).|
2227|Boolgeeda Iron Formation|69590|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Of Hamersley Basin. Events: Paterson Orogeny; Miles Orogeny.||Unit of Hamersley Group.|||Basaltic volcanic and sedimentary rock; interbedded with mudstone, siltstone, sandstone, and carbonate rock; metamorphosed at greenschist to amphibolite facies|
2227|Boolgeeda Iron Formation|69745|6|Mentioned|p273, 276, 287|||Crops out in the Mount Wall Fe deposit area, Hamersley Province. See also references to Boolgeeda Formation (p272, 275, 281).||Hamersley Group.||||
2227|Boolgeeda Iron Formation|69754|5|Briefly described|p315-p319, p330-p333, p336, p340|||Pilbara Craton. Exposed in the Hardey Syncline. Sedimentary facies are detailed.||||Conformably overlies the Woongarra Rhyolite. Conformably overlain by the Kungarra Formation.|Very finely bedded banded-iron formation, strongly magnetic cherty banded iron formation, greenish-black laminated iron formation, and weakly magnetic, green, millimetre-layered iron-formation.|
2227|Boolgeeda Iron Formation|70086|5|Briefly described|p196,202|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin. Depositional environment: deepwater BIF, sediment-starved. {Misspelt as Boolgeda on p216 Fig1].||Unit of Hamersley Group.||Uppermost unit of Hamersley Group. Overlain by Kungarra Formation, and locally by Meteorite Bore Member.|Banded iron formation.|
2227|Boolgeeda Iron Formation|70509|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. ||Unit of Hamersley Group.||Uppermost unit of Hamersley Group. Underlain by Woongarra rhyolite.||
2227|Boolgeeda Iron Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2445-2208 Ma||||Fine grained, finely laminated iron formation, mudstone, siltstone and numerous dolerite sills; metamorphosed.|
2227|Boolgeeda Iron Formation|71042|5|Briefly described|p66 fig 2|Paleoproterozoic|Paleoproterozoic|Oakover Basin.||Hamersley Group||||
2227|Boolgeeda Iron Formation|71112|4|Described|p69-73-76,79-80,83|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Exposed around the Hardey Syncline; exposed middle siliciclastic unit here preserves evidence for NE-ward paleoflow. Also well exposed around Turee Creek Syncline. Interpreted as a condensed section with the underlying Woongarra Volcanics (starved basin).||||Overlain by Kungarra Formation/ Turee Creek Group. Underlain by Wongarra Volcanics.|Banded iron formations with middle member of fine-grained siliciclastic turbidites.|
2227|Boolgeeda Iron Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, jaspilite, shale, iron formation|
2227|Boolgeeda Iron Formation|71513|6|Mentioned|p66,|||Pilbara Craton. Interpreted to have been deposited in a back-arc setting.||Hamersley Group||Overlies the Mt Sylvia and Mt McRae shales.|Banded-iron formation.|
2227|Boolgeeda Iron Formation|71550|5|Briefly described|p34-47|Siderian|Siderian|Geological province: Of Hamersley Basin. Depositional environment: deep-water, marine. Philippot et al. (2017) reported the occurrence of a 2 m-thick diamictite horizon within the Boolgeeda Iron Formation of drill core TCDP1, which shares the same characteristics as that identified at Boundary Ridge; suggesting the Boundary rdge diamictite unit represents a distinct glacial event separated from the overlying MBM by nearly 1500m of Kungarra shales. U-Pb zircon analysis of glacial diamictite from this study yield maximum age of 2.45 Ga.|c. 2.45 Ga|Unit of Hamersley Group.||Underlain by Wongarra Rhyolite.||03-SEP-19
2227|Boolgeeda Iron Formation|71808|4|Described|viii, ix, p41-p43, p47|||Hamersley Province. Up to approximately 200m thick. Glacial dropstones are present. BIFs are distinguished due to the lack of or poorly defined mesobanding. Subdivied into three informal members on the basis of lithology. See also p73, p117, p149, p156.||||Overlies the Woongarra Rhyolite. Conformably overlain by the Turee Creek Group.|Upper and lower, dark, flaggy to shaly banded iron formations with a central shale rich zone.|
2227|Boolgeeda Iron Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.|Max age 2445+/-5 Ma|Hamersley Group, upper|||Fine-grained, finely laminated iron-formation, mudstone, siltstone, and chert; metamorphosed.|
2227|Boolgeeda Iron Formation|72493|5|Briefly described|p30|||Hamersley Basin.||Uppermost Hamersley Group.||Overlies Woongarra Rhyolite. Is overlain by Kungarra Formation (Turee Creek Group).|Mostly BIF; minor epiclastic rocks.|
2227|Boolgeeda Iron Formation|72570|6|Mentioned|p2-3|||||Hamersley Group||Conformably overlain by the Kungarra Formation and the Woongarra Rhyolite.||
2227|Boolgeeda Iron Formation|72712|5|Briefly described|p3, p9, p10, p14, p17, p25, p42-44..|Siderian|Siderian|See also p46-47, p55. Shown as a revised formation in report. Ages are maximum depositional ages. Detrital zircon derived from erosion of underlying Woongarra Rhyolite.|</= 2445+/-5 Ma MDA.|Hamersley Group|Cave Hill Member|Disconformably overlies Woongarra Rhyolite. Gradationally to disconformably overlain by Kungarra Formation, Turee Creek Group.|Lower and uppper units of BIF separated by a shale unit. Minor volcaniclastic sandstone, siltstone and mudstone. Rare sandstone/diamicite.|14-JAN-21
2227|Boolgeeda Iron Formation|72758|5|Briefly described|p14 Tb.1, p23, p26,  p27.|||< 300m thick. BIF units are locally magnetic.||Hamersley Group||Conformably overlies Woongarra Volcanics and conformably underlies Turee Creek Group.|Laminated grey-brown to black, locally magnetite-bearing  BIF interbedded with chert and mudstone.|
2227|Boolgeeda Iron Formation|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Hamersley Group||Overlies the Woongarra Rhyolite, underlies the Turee Creek Group.|Banded iron formation.|
2227|Boolgeeda Iron Formation|73538|4|Described|p1-7, App TbS1|Siderian|Siderian|Hamersley Basin. Deposited during the Great Oxidation Event and the first major glacial event at about 2.45 Ga. Interpreted as a deep-water iron formation. [Presumably an informal subunit was referred to as the Boolgeeda diamictite]. Diamictite yielded a detrital zircon U-Pb age of 2460 +/- 9 Ma (Caquineau et al., 2018). Interpreted as being mainly derived from the underlying Hamersley and Fortescue groups.|2460 +/- 9 Ma|Hamersley Group||Underlain by Woongarra Rhyolite. Conformably overlain by Turee Creek Group including Kungarra Formation.|Mixed chemical and siliciclastic components including green mudstones and one glacial horizon.|
2250|Boonall Dolomite|22496|3|Fully described|p11||Neoproterozoic|Of the Albert Edward Group. Overlain by Douri Sandstone. Geological Province: Wolfe Basin.||||||14-APR-08
2250|Boonall Dolomite|22547|6|Mentioned|p28||Neoproterozoic III|Of the Albert Edward Group.||||||14-NOV-06
2250|Boonall Dolomite|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
2250|Boonall Dolomite|22901|6|Mentioned|76 fig 2|||||||||
2250|Boonall Dolomite|23314|5|Briefly described|331 Fig.2|||||||||
2250|Boonall Dolomite|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Albert Edward Group. Overlying unit Douri Sandstone. Underlying unit Elvire Formation. Wolfe Basin. Max. thickness: 100 m.||||||
2250|Boonall Dolomite|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
2250|Boonall Dolomite|23806|5|Briefly described|p1131|||Of the Albert Edward Group.||||||
2250|Boonall Dolomite|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Albert Edward Group. Overlies Elvire Formation. Geological Province: Wolfe Basin. Max Thickness: 100m. Pale grey to pale pink, medium to very fine-grained dolomitic mudstone and sandstone||||||09-MAR-05
2250|Boonall Dolomite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2250|Boonall Dolomite|32660|5|Briefly described|Table 6|||||||||
2250|Boonall Dolomite|32728|6|Mentioned|Fig.16|||See also Table 7||||||
2250|Boonall Dolomite|36551|6|Mentioned|Table 12|||||||||
2250|Boonall Dolomite|36888|4|Described|p214|||||||||
2250|Boonall Dolomite|36898|5|Briefly described|Table II|||||||||
2250|Boonall Dolomite|37927|6|Mentioned|Fig.2|||||||||
2250|Boonall Dolomite|38157|6|Mentioned|Table X|||||||||
2250|Boonall Dolomite|38243|6|Mentioned|p357|||||||||
2250|Boonall Dolomite|38988|6|Mentioned|p16|||||||||
2250|Boonall Dolomite|41429|6|Mentioned|p247|||See also p248||||||28-MAY-15
2250|Boonall Dolomite|43299|5|Briefly described|Map Legend||Neoproterozoic|Of Duerdin Group.||||||14-APR-08
2250|Boonall Dolomite|43303|5|Briefly described|Map Legend||Neoproterozoic|Of Albert Edward Group.||||||14-APR-08
2250|Boonall Dolomite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
2250|Boonall Dolomite|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 30 m thick.||Albert Edward Group||Overlies Elvire Formation (conformably). Overlain by Timperley Shale (conformably).|Yellow and grey dolomite; minor dolomite breccia, shale and siltstone.|07-MAR-18
2250|Boonall Dolomite|44317|4|Described|Table 3, p.7||Adelaidean|||||||
2250|Boonall Dolomite|44318|14|Not recorded|map legend||Adelaidean|Adelaidean||||||
2250|Boonall Dolomite|44324|14|Not recorded|p.10||Adelaidean|Tb.2. (Adelaidean) of Albert Edward Group.||||||
2250|Boonall Dolomite|44325|14|Not recorded|map legend||Adelaidean|||||||
2250|Boonall Dolomite|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
2250|Boonall Dolomite|45047|2|Defined|p95|Adelaidean|Adelaidean|See also p36.||||||28-MAY-15
2250|Boonall Dolomite|45140|3|Fully described|p59, Appx.p37|||Dow and Gemuts (1969). Unnamed basin NW of Birrindudu Basin. Named after Boonall Yard. [No type section details]. Up to 60m thick. Contains stromatolites.||Albert Edward Group.||Conformably overlies Elvire Formation locally. Is overlain conformably by Timperley Shale.|Dolomite; minor dolomitic conglomerate, dolomite breccia.|
2250|Boonall Dolomite|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
2250|Boonall Dolomite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Albert Edward Group. Geological Province: Wolfe Creek Basin. Yellow or grey laminated dolomite, dolorudite, and argillite.||||||
2250|Boonall Dolomite|63458|5|Briefly described|p871-874, p884-891, p893-894, p896-900 |Ediacaran|Ediacaran|60-100 m thick dolomitic unit. Described in great detail. ||Of the Albert Edward Group||Conformably overlies Elvire Formation. Correlated with Julie and (upper) Wonoka Formations. Is overlain conformably by Timperley Shale.|Basal laminated buff dolostone interbedded with flaggy dolomitic siltstone; grainstone and stromatolitic horizons mostly in uppermost horizons; discontinuous beds of graded and massive conglomerate.|
2250|Boonall Dolomite|63762|5|Briefly described|p19|||Of the Albert Edward Group.||||||07-FEB-11
2250|Boonall Dolomite|64104|6|Mentioned|p62 fig.1, p73 Tb.3, p74|Neoproterozoic|Neoproterozoic|||Albert Edward Group||Overlies Elvire Formation.||
2250|Boonall Dolomite|67484|6|Mentioned|p294, p295 Fig.2, p296|Ediacaran|Ediacaran|East Kimberley.||Of the Albert Edward Group.||Correlated with Egan, Julie and Wonoka Formations. Overlain by Timperley Shale. Underlain by Elvire Formation.||
2250|Boonall Dolomite|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Elvire Formation. Is overlain by Timperley Shale.||
2250|Boonall Dolomite|68138|5|Briefly described|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Albert Edward Group.||Correlated with Egan Formation.||
2250|Boonall Dolomite|68244|4|Described|p659-660,666-671|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Glaciogenic unit deposited during Egan Glaciation. ~40m thick.||Unit of Albert Edward Group.||Overlain by Timperley Shale. Underlain by Elvire Formation. Correlative to Egan Formation.|Basal interbedded laminated buff dolomite and flaggy dolomitic siltstone; common upper intraclastic, peloidal, oolitic and stromatolitic grainstone. Discontinuous lenticular  beds of graded and massive conglomerate above laminated dolomite.|
2250|Boonall Dolomite|68277|6|Mentioned|p103|Neoproterozoic|Neoproterozoic|E Kimberley.||||Correlated with Egan Formation.||
2250|Boonall Dolomite|68473|6|Mentioned|p531|||||Albert Edward Group||||
2250|Boonall Dolomite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Of Albert Edward Group.|||Yellow or grey laminated dolostone, dolorudite, and mudstone|30-JUL-15
2250|Boonall Dolomite|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Yellow or grey laminated dolostone, dolorudite and mudstone.|
2250|Boonall Dolomite|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Albert Edward Group.|||Yellow or grey laminated dolostone, dolorudite, and mudstone|
2250|Boonall Dolomite|70154|6|Mentioned|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group||||
2250|Boonall Dolomite|71146|6|Mentioned|p21|Ediacaran|Ediacaran|Partially equivalent to the Egan Formation. ||||Overlain by the Albert Edward Group.||
2250|Boonall Dolomite|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Yellow or grey laminated dolostone, dolorudite, and mudstone|
2250|Boonall Dolomite|73255|6|Mentioned|p532, p534|Ediacaran|Ediacaran|Contains the stromatolite Tungussia julia. 567 Ma age for the top of the unit.|567 Ma|Albert Edward Group||Overlies the Elvire Formation, underlies the Timperley Shale.|Limestone with domical stromatolites.|
2261|Boongal Formation|23045|6|Mentioned|291 fig 8|||Of the Fortescue Group.||||||16-JAN-07
2261|Boongal Formation|23570|3|Fully described|p83|Archean|Archean|See also p232 App. 1.  Of Fortescue Group. Lat. equiv.of Kylena Formation.  Replaces Boongal Pillow Lava Member (de la Hunty,1965). Overlain by Pyradie Formation; underlain by Hardey Formation.  Max.thick: 1200m.  Geological Province: Pilbara Craton.||||||07-NOV-08
2261|Boongal Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Underlain by Hardey Formation. Geological Province Hamersley Basin.||||||07-NOV-08
2261|Boongal Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Hardey Formation. Overlain by Pyradie Formation. Flow lava. Geological Province: Hamersley Basin.||||||07-NOV-08
2261|Boongal Formation|42471|5|Briefly described|p5, p4|||Equivalent to Boongal Pillow Lava Member of Mount Jope Volcanics (1965, 1968).||||||
2261|Boongal Formation|42472|5|Briefly described|Map legend|Archean||||||||23-DEC-09
2261|Boongal Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
2261|Boongal Formation|42744|4|Described|p3|||||||||
2261|Boongal Formation|43119|4|Described|p6|||Of the Fortescue Group.||||||16-JAN-07
2261|Boongal Formation|43262|5|Briefly described|Map Legend||Archean|Of the Fortescue Group.||||||07-NOV-08
2261|Boongal Formation|43290|4|Described|p5||Archean|Of the Fortescue Group.||||||07-NOV-08
2261|Boongal Formation|60706|5|Briefly described|p625 Fig.3||Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
2261|Boongal Formation|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Overlies the Hardey Formation. Geological Province: Pilbara Craton.||||||07-NOV-08
2261|Boongal Formation|62129|3|Fully described|p6, p7, p21|Archaean|Archaean|Of Fortescue Group. Conformably overlies Hardey Formation, overlain conformably by Pyradie Formation. Thickness: 1000m. Geological Province: Hamersley Basin. Submarine mafic volcanic rocks.||||||17-DEC-12
2261|Boongal Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Pillowed and massive metaconglomerate, metabasalt, metamorphosed volcanic sandstone, and metabasaltic breccia.||||||23-DEC-09
2261|Boongal Formation|63367|5|Briefly described|p231 Fig.1.|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Equivalent to Kylena Formation.||
2261|Boongal Formation|64384|5|Briefly described|p29 Tb. 5|Archean|Archean|Of the Fortescue Group. Geological province: southern Hamersley Basin.||||||07-FEB-11
2261|Boongal Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group. Pillowed and massive basaltic flows; basaltic breccia; siltstone; mudstone; minor chert; metamorphosed.||||||09-DEC-08
2261|Boongal Formation|64724|5|Briefly described|p42 Fig. 3|Neoarchean|Neoarchean|Hamersley Basin unit.||Of Fortescue Group.||||02-APR-12
2261|Boongal Formation|66217|5|Briefly described|p45.|||Fortescue Basin.||Unit in Fortescue Group.|||Subaqueous basaltic to komatiitic lavas and volcaniclastic rocks.|
2261|Boongal Formation|67025|6|Mentioned|p322 Table 3.|||Hamersley Basin. Mean bulk susceptibility of this and other units is discussed in this article.||||||
2261|Boongal Formation|67201|4|Described|p28-30|||In northern Pilbara Craton, southern Fortescue Basin, South Pilbara Sub-basin.||Fortescue Group||Equivalent to Kylena Formation.|Dominated by tholeiitic basalts, with massive flows, associated with pillow lava and hyaloclastite breccia.|
2261|Boongal Formation|68101|5|Briefly described|p2 Fig.1|||South Pilbara Sub-basin.||Fortescue Group.||Equivalent to Kylena Formation.||
2261|Boongal Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Fortescue Group.|||Pillowed and massive basaltic flows with basaltic breccia, siltstone, and mudstone; minor chert; metamorphosed.|06-MAY-14
2261|Boongal Formation|69080|5|Briefly described|p687, p693|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Overlies Hardey Formation. Is overlain by Pyradie Formation.||
2261|Boongal Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Pillowed and massive basaltic flows; basaltic breccia; siltstone; mudstone; minor chert; metamorphosed.|
2261|Boongal Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of South Pilbara Sub-basin, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Fortescue Group.|||Pillowed and massive basaltic flows; basaltic breccia; siltstone; mudstone; minor chert; metamorphosed|
2261|Boongal Formation|69301|5|Briefly described|p17 Fig.6, p18 Fig.7|||Pilbara Craton. Fortescue Basin. South Pilbara Sub-basin, Sequence 3.||Fortescue Group||||
2261|Boongal Formation|69792|6|Mentioned|p1096 Fig.1, p1106|||Described as the "supposed southern equivalent" of the Kylena Formation.||Unit in Fortescue Group.||||22-JUN-20
2261|Boongal Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2749-2730 Ma|||||
2261|Boongal Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt|
2261|Boongal Formation|71803|4|Described|p366, p368|||Pilbara Craton. An age of 2760 +/- 10 Ma is derived for the base of this unit from Arndt et al, 1991.||||Laterally equivalent to the Kylena Formation.|Abundant mafic lavas including both subaerial, subaqueous flows with mafic volcaniclastic rocks, lesser andesite and rhyolite and minor carbonates.|
2261|Boongal Formation|71808|5|Briefly described|p7|||Pilbara Craton. Basalt was deposited in both subaerial and submarine environments.||Fortescue Group|||Basalt and andesite.|
2261|Boongal Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|South Pilbara Sub-basin, Fortescue Basin.||Fortescue Group, sequence 3|||Pillowed and massive basaltic flows with basaltic breccia, siltstone and mudstone; minor chert; metamorphosed.|
2261|Boongal Formation|72712|5|Briefly described|p8, p7, p10 Fig.6, p11 Fig.8.|Neoarchean|Neoarchean|Formation is about 1km thick in study area.|max. age c. 2745 Ma|Fortescue Group.||Conformably overlies Hardey Formation. Conformably underlies Pyradie Formation and is equivalent to Kylena Basalt/Formation|Includes massive submarine basalt and pillow basalt with minor hyaloclastite breccia and mafic volcaniclastic rock.|
2261|Boongal Formation|73538|6|Mentioned|p4|Neoarchean|Neoarchean|Written as Kylena Formation / Boongali Formation. An age of 2760 +/- 10 Ma was reported by Mole et al. (2018) for these units.|2760 +/- 10 Ma|Fortescue Group||Underlain by Hardey Formation. Overlain by Pyradie Formation / Tumbiana Formation.|Mafic volcanics.|
2266|Boongerooda Greensand Member|24094|5|Briefly described|p275|||Name used interchangably with Boongerooda Greensand. Geological Province: Carnarvon Basin||||||16-MAR-05
2266|Boongerooda Greensand Member|24455|5|Briefly described|p327|||Of the Cardabia Calcarenite.  Geological Province: Carnarvon Basin.||||||22-MAR-05
2266|Boongerooda Greensand Member|41271|4|Described|p166|||||||||
2266|Boongerooda Greensand Member|61155|5|Briefly described|p15|Late Paleocene|Late Paleocene|Of the Cardabia Calcarenite. Age: 61.5-60Ma. Geological Province: Carnarvon Basin/onshore.||||||03-MAR-10
2301|Bora Monzogranite|42705|5|Briefly described|map legend|Archean||||||||07-NOV-08
2301|Bora Monzogranite|42988|5|Briefly described|Map Legend|||||||||
2301|Bora Monzogranite|42989|5|Briefly described|p12|||||||||
2301|Bora Monzogranite|43101|5|Briefly described|p25|||||||||
2301|Bora Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
2301|Bora Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmbo]  Equigranular, medium-grained biotite monzogranite.||||||02-FEB-05
2301|Bora Monzogranite|65204|6|Mentioned|p17 Tbl.2,|Neoarchean||0.5-3mm grains; equigranular||||||
2301|Bora Monzogranite|65264|5|Briefly described|p46 Appdx. 1|Archean|Archean|Medium-grained, equigranular biotite monzogranite; scattered mafic enclaves and strong foliation.||||||07-FEB-11
2301|Bora Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained, equigranular biotite monzogranite; scattered mafic enclaves and strong foliation.|05-AUG-15
2301|Bora Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained, equigranular biotite monzogranite; scattered mafic enclaves and strong foliation.|
2301|Bora Monzogranite|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv.|3010-2600 Ma (inferred)||||Medium-grained, equigranular biotite monzogranite; scattered mafic enclaves and strong foliation|
2312|Borde Formation|5952|5|Briefly described|p215 Fig. 5|||Appears as Borde in figure. Geological Province: Bonaparte Basin.||||||01-MAR-10
2312|Borde Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Cretaceous|Bathurst Island Group.||||||01-MAR-10
2312|Borde Formation|42053|4|Described|p45|||||||||01-MAR-10
2312|Borde Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
2312|Borde Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
2312|Borde Formation|60634|6|Mentioned|p1168 Fig.3. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||
2312|Borde Formation|64697|5|Briefly described|p84 Fig.2|Late Cretaceous|Late Cretaceous|||||||
2314|Border Creek Formation|13234|6|Mentioned|p250 Fig.2,|||||||Overlies Tanmurra Formation onshore.||
2314|Border Creek Formation|23820|5|Briefly described|p202 Fig.2|Late Carboniferous|Late Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
2314|Border Creek Formation|32648|6|Mentioned|p32|||Westphalian.||||||
2314|Border Creek Formation|32662|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
2314|Border Creek Formation|32663|4|Described|Table 2|||U.Carb.||||||
2314|Border Creek Formation|32664|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|Briefly described in notes||||||
2314|Border Creek Formation|32699|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Quartz sandstone, conglomerate, siltstone.||||||02-DEC-04
2314|Border Creek Formation|32701|4|Described|Table 2|||U.Carb. See also p16||||||26-JUL-06
2314|Border Creek Formation|32870|5|Briefly described|p48|||See also p53||||||26-JUL-06
2314|Border Creek Formation|33622|6|Mentioned|p89|||Late Carb.||||||
2314|Border Creek Formation|34085|6|Mentioned|Cor.chart|Stephanian|Westphalian|||||||26-JUL-06
2314|Border Creek Formation|36257|6|Mentioned|Table 2.1|||||||||
2314|Border Creek Formation|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
2314|Border Creek Formation|36551|6|Mentioned|Table 16|||||||||
2314|Border Creek Formation|36596|6|Mentioned|Text Fig.2|||||||||
2314|Border Creek Formation|36890|3|Fully described|p381|||||||||
2314|Border Creek Formation|36904|6|Mentioned|p9|||||||||
2314|Border Creek Formation|37926|6|Mentioned|p499|||||||||
2314|Border Creek Formation|39827|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
2314|Border Creek Formation|40301|6|Mentioned|Fig.2|||||||||
2314|Border Creek Formation|40494|4|Described|p19|||||||||
2314|Border Creek Formation|41532|6|Mentioned|Fig.15|||||||||
2314|Border Creek Formation|41598|5|Briefly described|p420|||||||||
2314|Border Creek Formation|41690|5|Briefly described|p5|||Mention Fig.2||||||
2314|Border Creek Formation|41839|6|Mentioned|p32|||Superseded by Border Creek Member||||||
2314|Border Creek Formation|41864|6|Mentioned|p131, 130|||Of Roberts (1968). Status changed to Border Creek Member of the Point Spring Sandstone.||||||
2314|Border Creek Formation|41865|5|Briefly described|Map legend|early Namurian|late Visean|||||||
2314|Border Creek Formation|42442|6|Mentioned|p11|||Of Point Spring Sandstone. See also Fig.3, p4.||||||26-JUL-06
2314|Border Creek Formation|42547|4|Described|p103|||||||||
2314|Border Creek Formation|45038|2|Defined|p.108||Late Carboniferous|See also Plates and Figures.||||||
2314|Border Creek Formation|45039|4|Described|p6|||See also pp7,26. Upper Carboniferous.||||||26-JUL-06
2314|Border Creek Formation|45050|6|Mentioned|p12|||See also p7,8,9,12 etc.||||||26-JUL-06
2314|Border Creek Formation|45056|6|Mentioned|p7|||||||||
2314|Border Creek Formation|45063|6|Mentioned|p8|||See also p19 & Fig. 3. U.Carb.||||||26-JUL-06
2314|Border Creek Formation|45097|5|Briefly described|p20|||Microfloral assemblage ? reworked. Correlation chart.||||||
2314|Border Creek Formation|45169|4|Described|p6|||||||||
2314|Border Creek Formation|46849|6|Mentioned|Fig. 2|||||||||
2314|Border Creek Formation|47040|6|Mentioned|Fig.3|||||||||
2314|Border Creek Formation|48886|14|Not recorded|Map||Late Carboniferous|U.Carb||||||
2314|Border Creek Formation|49637|5|Briefly described|Fig. 6|Late Carboniferous|Late Carboniferous|Geological Province: Bonaparte Basin.||||||07-FEB-11
2314|Border Creek Formation|60364|4|Described|p186 Fig.3|||Disconformably overlies Burt Range Formation, Zimmerman Sandstone and Septimus Limestone. Geological Province: Bonaparte Basin.||||||11-MAY-05
2314|Border Creek Formation|60682|4|Described|p25|||Has been used for Waggon Creek Formation and Point Spring Sandstone.||||||
2314|Border Creek Formation|61542|5|Briefly described|p277 Fig. 2|Stephanian|Westphalian|Onshore unit of Wadeye Gp. Regarded as part of Point Spring Sst. by Mory and Beere(1988) but actually overlies it. Interpreted as onshore equivalent of Kuriyippi Fm. Geol.prov: onshore Bonapart Basin/Petrel-Sub-basin. More. See also p282 Fig. 8.||||||28-SEP-11
2314|Border Creek Formation|65382|6|Mentioned|p717 App. 2|Permian|Permian|Bonaparte Basin. 298 Ma.||||||
2314|Border Creek Formation|69452|4|Described|p36:9, 11-14, 17-18|||Veevers and Roberts (1968). Later Border Creek Member (Mory and Beere, 1988) of Point Spring Sandstone; subsequently reinterpreted by Gorter et al. (2005) as being part of Kulshill Group, and reinstated to Formation status. Petrel Sub-basin, Bonaparte Basin. Fluvial to deltaic deposits. Over 111m thick. Onshore. Exposed as prominent cliffs of jointed sandstone and flat-topped ridges. It is the western basin-margin equivalent of the Kuriyippi Formation.||Kulshill Group.||Unconformably overlies Langfield, Weaber and Wadeye Groups. Is overlain by Keep Inlet Formation, and unconformably by Treachery Formation. Is faulted against Enga Sandstone.|Sandstone, generally cross-bedded with occasional pebble beds, and conglomerate; minor interbedded siltstone.|12-JUL-16
2314|Border Creek Formation|69673|4|Described|p173|||||Kulshill Group|||Sandstone and conglomerate with lesser interbedded siltstone.|
2314|Border Creek Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Wadeye Group.|||Quartz sandstone, conglomerate, siltstone|
2329|Boreas suite|41988|6|Mentioned|p101|||||||||
2329|Boreas suite|70153|5|Briefly described|118947.1.pdf|Archean|Archean|Age derived from coarsed grained porphyritic granite sample (118947.1.pdf). Actually shown as 'Boreas suite'. Dated in 1996.|2637 +/- 8 Ma (U-Pb SHRIMP zircon; Nelson 1997).||||Includes undeformed, coarse-grained, porphyritic granite.|01-SEP-16
2378|Boulder Tuffite|33513|5|Briefly described|p32|||Stratigraphy and structure.||||||17-SEP-08
2378|Boulder Tuffite|33514|6|Mentioned|p19|||||||||
2394|Bow River Granite|14019|6|Mentioned|p19|||Of the Lamboo Complex.||||||
2394|Bow River Granite|22547|6|Mentioned|p11||Orosirian|Superseded by Paperbark supersuite and Sally Downs supersuite which, collectively along with the granitoids of the Hooper Complex, constitute the Bow River batholith.||||||14-NOV-06
2394|Bow River Granite|22741|6|Mentioned|P20|||||||||
2394|Bow River Granite|23125|5|Briefly described|Table.1|||||||||
2394|Bow River Granite|23383|6|Mentioned|p7|||Equivalent to the Bow River Granitoid of Ogasawara (1988).||||||25-JAN-05
2394|Bow River Granite|23599|6|Mentioned|p12|||||||||
2394|Bow River Granite|24173|6|Mentioned|p21|||Along with McIntosh Gabbro now grouped into Shepherds Bore Plutonic Complex.||||||06-APR-05
2394|Bow River Granite|30097|6|Mentioned|Table 24|||Also Table 27||||||
2394|Bow River Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2394|Bow River Granite|32660|5|Briefly described|Table 1|||||||||
2394|Bow River Granite|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
2394|Bow River Granite|32699|5|Briefly described|Map legend|Carpentarian|Carpentarian|Within the Lamboo Complex.  Coarse grained and porphyritic biotite granite.||||||02-DEC-04
2394|Bow River Granite|32701|4|Described|Table 1|||Carpentarian. Lamboo Complex.||||||18-FEB-08
2394|Bow River Granite|32728|5|Briefly described|p29|||See also Fig.3||||||
2394|Bow River Granite|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2394|Bow River Granite|33377|6|Mentioned|Table 1|||||||||
2394|Bow River Granite|33812|6|Mentioned|p2|||Dated||||||
2394|Bow River Granite|34834|6|Mentioned|p213|||||||||
2394|Bow River Granite|35484|6|Mentioned|p307|||||||||
2394|Bow River Granite|35950|6|Mentioned|p302|||||||||
2394|Bow River Granite|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2394|Bow River Granite|36551|6|Mentioned|p41|||See also p46.||||||26-JUL-06
2394|Bow River Granite|36885|4|Described|p175|||||||||
2394|Bow River Granite|36898|6|Mentioned|p183|||||||||
2394|Bow River Granite|37462|4|Described|Table 4.I|||||||||
2394|Bow River Granite|38482|6|Mentioned|Table 1|||||||||
2394|Bow River Granite|38900|6|Mentioned|p66|||||||||
2394|Bow River Granite|39827|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2394|Bow River Granite|40494|4|Described|p9|||||||||
2394|Bow River Granite|40811|6|Mentioned|p317|||||||||
2394|Bow River Granite|41158|5|Briefly described|p36|||Mention p59.||||||18-FEB-08
2394|Bow River Granite|41465|5|Briefly described|p9|||||||||
2394|Bow River Granite|41594|6|Mentioned|p46|||||||||
2394|Bow River Granite|41703|6|Mentioned|p231|||||||||
2394|Bow River Granite|41864|6|Mentioned|p64|||||||||
2394|Bow River Granite|41961|6|Mentioned|Table 1 P39|||||||||
2394|Bow River Granite|41976|5|Briefly described|p463|||||||||
2394|Bow River Granite|41977|4|Described|p471|||||||||
2394|Bow River Granite|41987|6|Mentioned|Fig.3 P73|||||||||
2394|Bow River Granite|42149|6|Mentioned|p704|||||||||
2394|Bow River Granite|42326|5|Briefly described|p9|||||||||
2394|Bow River Granite|42342|5|Briefly described|p22|||||||||
2394|Bow River Granite|43632|4|Described|p6||Proterozoic|Zircon age: 1850 Ma||||||
2394|Bow River Granite|43794|5|Briefly described|p320|||||||||
2394|Bow River Granite|43832|6|Mentioned|88||Paleoproterozoic|Age in the range 1880-1800 Ma.||||||07-NOV-08
2394|Bow River Granite|44155|4|Described|p234 Tb.3-2, p239, p240-241, p242 Tb.3-5|Paleoproterozoic|Paleoproterozoic|See also p243 Tb.3-6, p245-248, p254 Fig.3-40. East Kimberley. Prominent contact aureole. Late to post-tectonic faulting. Whole-rock Rb-Sr isochron age.|1815 +/- 14 Ma (Page, 1976).|Lamboo Complex||Intrudes Whitewater Volcanics, Halls Creek Group, Tickalara Metamorphics, Mabel Downs Granodiorite, McIntosh Gabbro. Is intruded by Violet Valley Tonalite.|Coarse-grained porphyritic or even-grained biotite or hornblende syenogranite, monzogranite and granodiorite.|
2394|Bow River Granite|44317|4|Described|Table 1||Proterozoic|||||||
2394|Bow River Granite|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
2394|Bow River Granite|44324|14|Not recorded|p.7||Proterozoic|Tb.1. (Proterozoic).||||||
2394|Bow River Granite|44325|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
2394|Bow River Granite|44363|5|Briefly described|p.19,20||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
2394|Bow River Granite|44364|14|Not recorded|map legend|||||||||
2394|Bow River Granite|44366|14|Not recorded|p.8||Proterozoic|Part of Lamboo Complex.||||||
2394|Bow River Granite|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Lamboo Complex.||||||
2394|Bow River Granite|44397|14|Not recorded|p.8, Table 1||Proterozoic|Lamboo Complex.||||||
2394|Bow River Granite|44398|14|Not recorded|map legend||Proterozoic|||||||
2394|Bow River Granite|45047|4|Described|p13|||See also p25. Age: 1854+-15my.||||||26-JUL-06
2394|Bow River Granite|45048|3|Fully described|p56|||See also p57-63. Carpentarian.||||||18-FEB-08
2394|Bow River Granite|45050|6|Mentioned|p7|||||||||
2394|Bow River Granite|45087|5|Briefly described|p26|||Chemical analyses||||||
2394|Bow River Granite|45112|5|Briefly described|p48|||||||||
2394|Bow River Granite|45140|6|Mentioned|p12|||Kimberley region.|c.1850 Ma.|||||
2394|Bow River Granite|46797|6|Mentioned|p81|||Dated||||||
2394|Bow River Granite|48938|3|Fully described|p13|||||||||
2394|Bow River Granite|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Part of Lamboo Complex. Intrudes the Hall Creek Group. Coarsely crystalline and porphyritic biotite granite.||||||07-NOV-08
2394|Bow River Granite|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Part of the Lamboo Complex. Intrudes Halls Creek Group and Whitewater Volcanics. Coarsely crystaline and porphyritic. Age: 1854 +/- 14Ma (Rb-Sr; Sweet, 1977). Geological Province: Halls Creek Orogen.||||||07-NOV-08
2394|Bow River Granite|60724|5|Briefly described|p14|||Proposed this be redefined as Bow batholith, more accurately reflecting the diversity of granitoid rocks. Bow batholith will include Sally Downs Tonalite, Violet Valley Tonalite and some of Mabel Downs Granodiorite as well as further newly defined units. ||||||
2394|Bow River Granite|63866|5|Briefly described|p105, p132|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Numeric age is interpreted as the crystallisation age.|1853 +/- 5 Ma (Worden et al, in review)|Paperbark Supersuite||||
2394|Bow River Granite|64104|6|Mentioned|p76, p77|Paleoproterozoic|Paleoproterozoic|Possible source of quartz-feldspar porphyry cobbles in Fargoo Formation. Limited exposure in the core of the Osmond Range.||||||
2394|Bow River Granite|64956|5|Briefly described|p2 Tb. 25, p94|Paleoproterozoic|Paleoproterozoic|Cryst. age: 1853+/-5Ma. Geological province: Halls Creek Orogen. Sample is a K-feldspar-megacrystic biotite granite.||||||07-FEB-11
2394|Bow River Granite|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Lamboo Complex, Halls Creek Orogen. Coarsely crystalline and porphyritic biotite granite.||||||30-JUL-15
2394|Bow River Granite|68244|6|Mentioned|p666|Paleoproterozoic|Paleoproterozoic|Lamboo Complex.|1857+\-5 Ma|Unit of Lamboo Complex.||Overlain unconformably by Landrigan Formation (Kuniandi Group).||21-JUN-19
2394|Bow River Granite|69099|5|Briefly described|ga_geochron.csv|Paleoproterozoic|Paleoproterozoic|Halls Creek Province|Rb/Sr 1834+/-32 Ma|||||
2394|Bow River Granite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Paleoproterozoic||1834- 2682 Ma|||||
2394|Bow River Granite|69417|6|Mentioned|p2:5|Orosirian|Orosirian|||||Intrudes Whitewater Volcanics.||12-JUL-16
2394|Bow River Granite|69422|4|Described|p7:1-3|Orosirian|Orosirian|Western Zone, Halls Creek Orogen. Considered to be comagmatic with the Whitewater Volcanics. SHRIMP U-Pb zircon age.|1853 +/- 5 Ma (Worden et al., 2008).|Paperbark Supersuite.||Intrudes Whitewater Volcanics.|Typically a pink to green-grey, coarsely crystalline and porphyritic biotite granite; phenocrysts of K-feldspar locally displaying rapakivi textures.|12-JUL-16
2394|Bow River Granite|69435|5|Briefly described|p20:3|Paleoproterozoic|Paleoproterozoic|Part of the basement to the Fitzmaurice Basin.|1853 +/- 3 Ma.|||Is overlain unconformably by Moyle River Formation.||12-JUL-16
2394|Bow River Granite|69673|6|Mentioned|p3, p60 fig 48|Orosirian|Orosirian||1853 +/- 3 Ma |||||
2394|Bow River Granite|70154|5|Briefly described|GA_geochron.csv||||||||Gneissic granites and metamorphics. Felsic weakly porphyritic granite.|
2394|Bow River Granite|70206|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Lamboo Complex|||Coarsely crystallite and porphyritic biotite granite.|
2394|Bow River Granite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Coarsely crystallite and porphyritic biotite granite.|
2394|Bow River Granite|71592|5|Briefly described|Appendix A.|||Halls Creek Orogen.|1853+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
2452|Boxies Bore Gabbro|41594|6|Mentioned|p39|||||||||
2511|Brassey Range Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
2511|Brassey Range Formation|22901|6|Mentioned|76 fig 2|||Geol province: Officer Basin.||||||08-SEP-08
2511|Brassey Range Formation|22907|5|Briefly described|42|||Of the Sunbeam Group. Geol. province: Officer Basin.||||||17-JUL-08
2511|Brassey Range Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
2511|Brassey Range Formation|24017|6|Mentioned|p11|||||||||
2511|Brassey Range Formation|24535|5|Briefly described|p2-3, 4|||Of Salvation Group. Previously included in Kahrban Subgroup and previously correlated with Sunbeam Group (Hocking and Jones, 2002).||||||26-NOV-13
2511|Brassey Range Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
2511|Brassey Range Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||17-JUL-08
2511|Brassey Range Formation|43492|3|Fully described|9|||||||||
2511|Brassey Range Formation|50188|4|Described|p11 Fig. 4|||Unconformably overlies Oldham Sandstone; also overlies Coonabildie Formation. Max.thickness: ~1250m. Geol.Prov: Officer Basin. Slightly redefined (see Abstract).||||||17-JUL-08
2511|Brassey Range Formation|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group. Quartz sandstone and subordinate siltstone, predominantly cross-bedded, in places pebbly; fluvial to coastal deposits.||||||28-MAY-04
2511|Brassey Range Formation|62453|5|Briefly described|p16, 22, 52|Mesoproterozoic|Mesoproterozoic|Underlies Spearhole Formation. Of the Salvation Group.||||||
2511|Brassey Range Formation|63866|4|Described|p163|Stenian|Ectasian|Bangemall Basin. SHRIMP age is interpreted as the maximum depositional age for this formation.|1229 +/- 85 Ma (SHRIMP U-Pb, Nelson, 2002)|Salvation Group||Overlies the Coonabildie Formation.|Sandstones.|
2511|Brassey Range Formation|64283|5|Briefly described|p51 Fig. 2|||Of Sunbeam Group. Conformably overlies Coonabildie Formation (Sunbeam Group). Unconformable on Oldham Sandstone. Geological Province: Officer Basin||||||07-FEB-11
2511|Brassey Range Formation|64286|5|Briefly described|p73 Fig. 2|||Geological province: Officer Basin.||||||07-FEB-11
2511|Brassey Range Formation|64580|4|Described|map legend||Mesoproterozoic|Of Salvation Group. Sandstone; lesser siltstone and shale.||||||17-NOV-08
2511|Brassey Range Formation|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Salvation Group. Quartz sandstone and subordinate siltstone, predominantly cross-bedded, in places pebbly; fluvial to coastal deposits.||||||
2511|Brassey Range Formation|64772|5|Briefly described|p13, Plate 1, p34 Fig.22|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group. Age: <1230ma. Sandstone; lesser siltstone and shale.||||||25-NOV-13
2511|Brassey Range Formation|64793|6|Mentioned|p283 fig 2, p285 fig 4|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
2511|Brassey Range Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin. Arenaceous. Part of Supersequence 1.||||||
2511|Brassey Range Formation|67195|4|Described|p10 fig 6, p19 table 1, p45, 48|Neoproterozoic|Neoproterozoic|Savory area, western Officer Basin. Thermal conductivity of 4.45 W/mK. See also App 1, App 2.||||Overlain by Spearhole Formation.|Medium grained to granular sandstone interbedded with shale and mudstone.|
2511|Brassey Range Formation|67200|5|Briefly described|app 2 p10||||||||Interbedded siltstone and sandstone.|
2511|Brassey Range Formation|69091|6|Mentioned|p202|Mesoproterozoic|Mesoproterozoic|Salvation Basin. Age: late Mesoproterozoic|||||Siliciclastic sedimentary rocks.|
2511|Brassey Range Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
2511|Brassey Range Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Salvation Basin. |max age 1229+/-85 Ma, min ~1080 Ma.|Salvation Group|||Sandstone; lesser siltstone and shale.|
2525|Breton Marl|14227|5|Briefly described|Enclos. 2|Maastrichtian|Maastrichtian|Of Coolyena Group.||||||07-FEB-11
2525|Breton Marl|42123|4|Described|p20|||||||||
2525|Breton Marl|42995|5|Briefly described|p20|||See also Table 1.||||||
2525|Breton Marl|43700|6|Mentioned|Fig.4,p26|||||||||
2525|Breton Marl|60709|5|Briefly described|p859|Maastrichtian|Maastrichtian|Geological Province: Perth Basin||||||
2530|Brewster Member|42053|5|Briefly described|Fig.3 P30|||||||||01-MAR-10
2530|Brewster Member|69297|6|Mentioned|p303, p305|Aptian|Berriasian|Barcoo and Seringapatam sub-basins of the Browse Basin. Deposited under a slope fan setting. ||Upper Vulcan Formation||Overlain by the Echuca Shoals Formation.||
2530|Brewster Member|70064|5|Briefly described|Northern Fig.2; p2. Yampi: Fig.2|Berriasian|Berriasian|See also Regional: Fig. 6; p4-6, p8. Central: Fig.2; p2. Caswell-Barcoo Sub-basins, Browse Basin. Wet gas-prone system reservoir which includes the Ichthys, Prelude/Concerto and Mimia accumulations, possibly sourced from Vulcan and Plover Formations.||Top of Upper Vulcan Formation.|||A thick sequence of clean, relatively high net/gross sands with mudstones; deposited by poorly confined, sand-rich, mid-slope grain flows or high-density turbidity currents on a deep-water ramp.|12-JUL-16
2550|Bridport Calcilutite|41200|2|Defined|p25-26|Holocene|Holocene|Underlies Becher Sand; overlies Tamala Limestone (unconf.), Cooloongup Sand (unconf.) and mud of Leschenault Formation (conf.). Max. thickness: 10m. Sequence of grey, structureless to bioturbated, calcareous (carbonate) mud with lesser carbonate mud.||||||17-MAY-18
2550|Bridport Calcilutite|41502|4|Described|Table 1|||||||||
2550|Bridport Calcilutite|61521|5|Briefly described|p4 Tb.1, p40|Holocene|Holocene|Grey, primarily carbonate sandy mud and mud infilling deep, relatively still-water environments of the central basin of Cockburn Sound. Age: <7,000 BP (semeniuk and Searle 1987). Geological Province: Rottnest Shelf region. See also p39 Tb.7, p41.||||||02-JUN-06
2550|Bridport Calcilutite|63454|5|Briefly described|p71 Tb. 3|||Grey calcilutite and shelly calcilutite.||||||08-AUG-07
2572|Bringo Shale|23279|6|Mentioned|p29|||||||||
2572|Bringo Shale|23816|4|Described|p244|Bajocian|Bajocian|Geological Province: Perth Basin. Of the Champion Bay Group. Underlying unit: Colalura Sandstone (conformable). Overlying unit: Newmarracarra Limestone (conformable). Max thickness: 2.4 m.||||||
2572|Bringo Shale|24020|5|Briefly described|p387|Bajocian|Bajocian|Geological Province: Perth Basin||||||16-MAR-05
2572|Bringo Shale|30948|6|Mentioned|Map legend|Bajocian|Bajocian|||||||
2572|Bringo Shale|31396|6|Mentioned|p1183|||See also P1184.||||||
2572|Bringo Shale|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
2572|Bringo Shale|32648|6|Mentioned|p32|||Champion Bay Gp.||||||
2572|Bringo Shale|32649|4|Described|p25|||See also Table 1||||||
2572|Bringo Shale|33022|6|Mentioned|p259|||||||||
2572|Bringo Shale|33166|6|Mentioned|p63|||Refers Arkell & Playford (1954)||||||
2572|Bringo Shale|34134|6|Mentioned|p482|||Middle Jurassic||||||
2572|Bringo Shale|34721|6|Mentioned|p286|||||||||
2572|Bringo Shale|35282|6|Mentioned|p31|||||||||
2572|Bringo Shale|36257|6|Mentioned|Table 2.1|||||||||
2572|Bringo Shale|36293|2|Defined|p150|Bajocian|Bajocian|||||||
2572|Bringo Shale|36890|3|Fully described|p244|||||||||
2572|Bringo Shale|41284|4|Described|p91|||||||||
2572|Bringo Shale|44144|4|Described|p506 Tb.4-21|Aalenian|Aalenian|Type Section: Bringo railway cutting, 28o44'54''S 114o50'54''E. 10m thick shallow marine restricted circulation sediments.||Champion Bay Group||Conformably overlies Colalura Sandstone. Overlain by Newmarracarra Limestone conformably.|Black shale with thin yellow phosphatic bands.|
2572|Bringo Shale|61811|4|Described|pp29-31, p62.|Middle Jurassic|Middle Jurassic|Type section in rail cutting, c. 24 km east of Geraldton; further details in Appendix 1.||Unit in Champion Bay Group.||Overlies Colalura Sandstone. Is overlain by Newmarracarra Limestone.|Friable black shale with thin yellow phosphate bands; containing palynomorphs, foraminifera and vertebrate remains.|
2572|Bringo Shale|64635|5|Briefly described|p16 |Middle Jurassic|Middle Jurassic|||Of the Champion Bay Group.||||
2592|Broadhurst Formation|22716|6|Mentioned|p239|Neoproterozoic|Neoproterozoic|||||||
2592|Broadhurst Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Throssell Group, Yeneena Basin.||||||
2592|Broadhurst Formation|23590|3|Fully described|p9|||Of Throssell Group. Underlain by Coolbro Sandstone.||||||24-JUL-07
2592|Broadhurst Formation|23594|4|Described|p21|Neoproterozoic|Mesoproterozoic|Of Throssell Group. Underlying unit Coolbro Sandstone. Geological Province: Yeneena Basin.||||||
2592|Broadhurst Formation|23602|4|Described|p15|||Of Throssell Group. Underlain by Coolbro Sandstone.||||||24-JUL-07
2592|Broadhurst Formation|23729|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Throssell Group. Geological Province: Yeneena Basin.||||||
2592|Broadhurst Formation|23730|4|Described|p10|Neoproterozoic|Mesoproterozoic|Of Throssell Group. U'lying unit Coolbro Sandstone. Geological Province: Yeneena Basin.||||||
2592|Broadhurst Formation|23745|4|Described|p16|Neoproterozoic|Mesoproterozoic|See also page 7 Fig 5. Of Throssell Group. Geological Province: Yeneena Basin. Max. thickness: 3000 m.||||||
2592|Broadhurst Formation|23746|4|Described|p24|Neoproterozoic|Mesoproterozoic|Of Throssell Group.||||||
2592|Broadhurst Formation|23760|4|Described|p22|Neoproterozoic|Mesoproterozoic|Of Throssell Group. Geological Province: Yeneena Basin.||||||
2592|Broadhurst Formation|23900|4|Described|p1535, p1537 Fig.2|Proterozoic|Proterozoic|Conformably overlies the Coolbro Sandstone. Unconformably overlain by the Isdell Formation. Geological Province: Paterson orogen||||||
2592|Broadhurst Formation|24025|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of the Throssell Group.  Geological Province: Pilbara Craton.||||||
2592|Broadhurst Formation|24194|4|Described|p898, p899 Fig.2, p900, Fig.3|Proterozoic|Proterozoic|Dolomite, carbonaceous, pyrite- and pyrrhotite- bearing shale with minor sandstone. Parent: Throssell Group. Underlying Unit: Coolbro Sandstone. Geological Province: Yeneena Basin.||||||28-JUL-08
2592|Broadhurst Formation|24594|5|Briefly described|p601|Neoproterozoic|Mesoproterozoic|Of the Throssell Group.  Shallow marine to fluvial carbonate unit.  Geological Province: Yeneena Basin (Paterson Orogen).||||||09-JUL-13
2592|Broadhurst Formation|33849|4|Described|p124|||||||||
2592|Broadhurst Formation|36551|6|Mentioned|Table 22|||||||||
2592|Broadhurst Formation|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
2592|Broadhurst Formation|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
2592|Broadhurst Formation|37212|3|Fully described|p12|||||||||
2592|Broadhurst Formation|37214|6|Mentioned|p6|||||||||
2592|Broadhurst Formation|37460|4|Described|Table3.VII|||||||||
2592|Broadhurst Formation|37707|6|Mentioned|Table I|||||||||
2592|Broadhurst Formation|42278|6|Mentioned|p33|||||||||
2592|Broadhurst Formation|42702|5|Briefly described|map legend|Proterozoic||||||||
2592|Broadhurst Formation|42730|5|Briefly described|p17|||Yeneena Group.||||||28-JUL-08
2592|Broadhurst Formation|43118|4|Described|p21|||of Yeneena Group||||||
2592|Broadhurst Formation|43278|5|Briefly described|p644,Fig.2.||Neoproterozoic|Of Yeneena Group.||||||28-JUL-08
2592|Broadhurst Formation|43348|3|Fully described|p10|||Of Yeneena Group. High mineral potential, Pb-Zn, Cu and U-Cu.||||||29-SEP-15
2592|Broadhurst Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||17-FEB-10
2592|Broadhurst Formation|43848|5|Briefly described|Map Legend||Proterozoic|||||||
2592|Broadhurst Formation|43867|5|Briefly described|Fig.2 p201|||Shown as part of informal Lower Yeneena Sub-Group.||||||
2592|Broadhurst Formation|44139|5|Briefly described|p277-280, p282|Neoproterozoic|Neoproterozoic|Williams et al. (1976). 0-1000 m. Shale, graphitic shale, siltstone; minor sandstone, dolomite. Central zone of Yeneena Basin, transitional downwards to Coolbro Sandstone; broadly equivalent to Waroongunyah, Brownrigg and Yandanunyah Formations; conformably overlain by Choorun or Isdell Formations. Mineralized. 900-750 Ma (Pb model ages on galena; Fletcher, pers. comm., 1986).| | ||||05-MAR-18
2592|Broadhurst Formation|44189|5|Briefly described|Map legend||Proterozoic|||||||
2592|Broadhurst Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
2592|Broadhurst Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
2592|Broadhurst Formation|50436|6|Mentioned|p1.1|||Of the Throssell Group.||||||
2592|Broadhurst Formation|50544|4|Described|p56-57|Neoproterozoic||Top unit of the Throssell Group.  Transgressive shallow marine deposit.  Conformably overlies the Coolbro Sandstone.  Max. thickness: est. 2500m.||||||
2592|Broadhurst Formation|50555|5|Briefly described|Map legend||Mesoproterozoic|Of the Throssell Group (Yeneena Supergroup).  Shale, siltstone, mudstone, and fine to medium-grained sandstone.  Age: <1060Ma.  Geological Province: Yeneena Basin.||||||23-DEC-09
2592|Broadhurst Formation|60470|4|Described|p4 Fig. 2, p7, 10-11, 12, 14-15|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Throssell Range Group.  Transitional contact with underlying Coolbro Sandstone. Shale, carbonate rocks, and turbidite units. Hosts Cu, Pb, Zn mineralization.||||||
2592|Broadhurst Formation|62453|4|Described|p5 Fig. 3, 67|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Throssell Range Group. Conformably overlies Coolbro Sandstone. Thickness: 2000m. Shale, siltstone, sandstone, wacke, dolomite, limestone.  ||||||
2592|Broadhurst Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Throssell Range Group. Geological Province: Yeneena Basin (Centralia Superbasin). Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone and fine-grained sandstone.||||||23-JUL-07
2592|Broadhurst Formation|64283|5|Briefly described|p54|||Of the Throssell Group. Overlies the basal Coolbro Sandstone. Comprises carbonaceous shale, siltstone, turbidite and carbonate units.||||||07-FEB-11
2592|Broadhurst Formation|64580|4|Described|map legend||Neoproterozoic|Of Throssell Range Group. Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone.||||||09-DEC-08
2592|Broadhurst Formation|64725|5|Briefly described|p74.|||Host to the stratabound epigenetic Cu (with minor Zn) Nifty deposit.||Unit in Throssell Range Group.|||Carbonates, shale.|
2592|Broadhurst Formation|64777|4|Described|p2|Neoproterozoic|Neoproterozoic|Model Pb ages from Pb-isotope analyses of galena in the formation gave ages of 905-550 Ma (Hickman and Clarke, 1994, Hickman and Bagas 1998). Suggested here that these ages may be wrong.|905-550 Ma|Of the Throssell Range Group.|||Shale, carbonate rocks, and turbidite units.|
2592|Broadhurst Formation|64941|5|Briefly described|p27, p29|Neoproterozoic|Tonian|In lower part of Yeneena Basin. Hosts Nifty Cu deposit. Age: 791+/-42 Ma pooled regression age with data somewhat scattered, Sm-Nd dating of apatite; and, apparent ages between 850 and 600 Ma, U-Pb apatite.|see comments|||Overlies Coolbro Sandstone.|Siltstone dominated; deposit hosted by chloritic, carbonaceous, and locally pyritic, shale with localized lenses of dolostone.|
2592|Broadhurst Formation|64943|5|Briefly described|p19 ,24, 26, 35, 37|Neoproterozoic||Shows Paterson Orogen D5 deformation. Of Throssell Group. Includes pelites and carbonates. Minimum age from epigenetic galena mineralisation: 900 Ma||||||
2592|Broadhurst Formation|65403|4|Described|p13, p18.|||Deposition probably in an anoxic pelagic environment, affected by periodic turbidity currents towards its base. Mineralisation is hosted by D4 structures (Miles Orogeny).|c.900 Ma minimum.|Unit in Throssell Group.||Conformably overlies Coolbro Sandstone.|Carbonaceous, pyritic and dolomitic shale and sandstone.|29-SEP-15
2592|Broadhurst Formation|65454|4|Described|p7-8, p10, p13, p22-23, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of Throssell Range Group. Thinly laminated sandstones, siltstones and black shales with discontinuous carbonate lenses that generally fine upwards. Correlative of Waters Formation. Hosts stratabound Cu deposits.||||||
2592|Broadhurst Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Throssell Range Group. Overlies Coolbro Sandstone. Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone. Age: older than Miles Orogeny (c.720). Province: Yeneena Basin (Centralian Superbasin)||||||26-FEB-13
2592|Broadhurst Formation|65826|4|Described|p1, pp12-13, pp17-18.|Neoproterozoic|Neoproterozoic|Outcrops around the Nifty mine and Goosewhacker copper prospect; hosts the Nifty Cu-Pb-Zn stratabound epigenetic deposit. Three types of copper mineralization: primary chalcopyrite, secondary silicified carbonate-hosted copper, and secondary shale-hosted mineralization. High-grade ore is best developed in carbonate beds below shale beds. The disseminated pyrrhotite gives the Formation a distinctive aeromagnetic signature. The unit hosts several other prospects.||Unit in Throssell Range Group.||Conformably overlies Coolbro Sandstone.|Carbonaceous shale and siltstone, dark grey tp black, dolomitic, thinly laminated; thin interbedded siltstone (micaceous and chloritic), shale (locally chloritic, thinly laminated, barite casts) and fine-grained sandstone. Local pyrite/pyrrhotite.|
2592|Broadhurst Formation|67202|3|Fully described|p7, p39, p43, p57-59, p61-63, p65, p93|Neoproterozoic|Neoproterozoic|See also p115, p117-119, p121-123, p132-133, p149, p155-157, p161, p163-166, p169-179, p182-188, p203, p208, p219, p221, p223-224, p226, p229, p232, p234, p238, p241, p244-250, p253, p272-273, p277-281. Yeneena Basin. An aquifer supplying water to the Nifty Cu-mining community (the Cu deposit is described in great detail). Sulfide-rich beds produce aeromagnetic highs. Thickness estimated at 2-3 km. Generalised lithological column. Conductivity discussed, imaged and modelled. Associated with (Cu-)U mineralisation, particularly at/near contact with Coolbro Sandstone (described in detail). May be associated with the Warrabarty Zn-Pb deposit (described). Said to be a unit of Yeneena Group on p232. Geochemistry discussed.||Throssell Range Group.|Nifty Member.|Overlain by Paterson Formation and, underlain conformably, Coolbro Sandstone. Is overlain by/faulted against Isdell Formation. Correlated with Waters Formation. Is faulted against Tarcunyah Group.|Lower and upper sections are dominantly carbonaceous shale/pelitic schist, beds of limestone and dolomite, and beds with up to 10% pyrite and pyrrhotite; with an intervening interval of argillaceous turbiditic greywacke and sandstone. Local basalt.|17-JUL-20
2592|Broadhurst Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||||||
2592|Broadhurst Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Mesoproterozoic|||Throssell Range Group||Overlies Coolbro Sandstone|Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone. Dolostone and silicifed dolostone, limestone, chert, sandstone and wacke.|
2592|Broadhurst Formation|69185|5|Briefly described|500k_geologyp08_lut.csv||Neoproterozoic|||Unit of Throssell Range Group.|||Undivided; carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone|
2592|Broadhurst Formation|69590|4|Described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Geological province: Paterson Orogen. Of Yeneena Basin. Events: Miles Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|911-650 Ma (inferred)|Unit of Throssell Range Group.|||Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone; dolostone and limestone; massive to thinly bedded; chert, stromatolitic dolostone.|
2592|Broadhurst Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||siltstone, crystalline dolostone/dolomite, basalt, sandstone|
2592|Broadhurst Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Yeneena Basin.||Throssell Range Group.|||Carbonaceous shale and siltstone, pyritic and pyrrhotitic shale, siltstone, and fine-grained sandstone.|
2602|Brockman Iron Formation|22689|6|Mentioned|139|||Of Hamersley Group,  Hamersley Basin.||||||
2602|Brockman Iron Formation|22701|5|Briefly described|Fig2,p39|Neoarchean|Neoarchean|~2470 +/- 4 Ma. Hamersley Group, Hamersley Basin. Overlies Mount McRae Shale. Overlain by Weeli Wolli Iron Formation||||||07-NOV-08
2602|Brockman Iron Formation|22716|6|Mentioned|p232|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
2602|Brockman Iron Formation|22814|6|Mentioned|p258|||||||||
2602|Brockman Iron Formation|23045|6|Mentioned|289|||Parent Hamersley Group||||||
2602|Brockman Iron Formation|23046|6|Mentioned|183|||Deposition commenced 2480 Ma||||||
2602|Brockman Iron Formation|23047|6|Mentioned|34|||Of the Hamersley Group. Hamersley Province.||||||10-FEB-09
2602|Brockman Iron Formation|23126|5|Briefly described|p383 Fig.3|||||||||
2602|Brockman Iron Formation|23127|5|Briefly described|p375 Fig.1, p377|||||||||
2602|Brockman Iron Formation|23150|5|Briefly described|p24|||of Hamersley Basin.||||||
2602|Brockman Iron Formation|23194|5|Briefly described|p41|||Hosts enriched hematite ores and BIF, shale and chert. Hamersley Group.||||||14-NOV-06
2602|Brockman Iron Formation|23205|6|Mentioned|p403|||of Hamersley Range.||||||
2602|Brockman Iron Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Hamersley Group.||||||
2602|Brockman Iron Formation|23354|5|Briefly described|315|||||||||
2602|Brockman Iron Formation|23536|4|Described| Fig 2 p 429|||also see Fig 1 p 428.||||||
2602|Brockman Iron Formation|23570|5|Briefly described|p27|||Geological Province: Pilbara Craton||||||
2602|Brockman Iron Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Overlying unit Weeli Wolli Formation.||||||07-NOV-08
2602|Brockman Iron Formation|23612|5|Briefly described|p840|Archean|Archean|||||||07-NOV-08
2602|Brockman Iron Formation|23808|6|Mentioned|p9|||||||||
2602|Brockman Iron Formation|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
2602|Brockman Iron Formation|23890|5|Briefly described|p5 Fig.2|||Of Hamersley Group. Age: 2470+/-4Ma (U-Pb SHRIMP).  Geological Province: Hamersley Basin.||||||
2602|Brockman Iron Formation|23936|4|Described|Tb.1|Paleoproterozoic|Archean|Age: c.2.47 Ga. Geological Province: Pilbara Craton. Overlying Unit: Weeli Wolli Iron Formation. Underlying Unit: McRae Shale. Parent: Hamersley Group.||||||01-MAR-10
2602|Brockman Iron Formation|24025|5|Briefly described|p35|||Of Hamersley Group.  Geological Province: Pilbara Craton.||||||
2602|Brockman Iron Formation|24041|4|Described|p491|Paleoproterozoic|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
2602|Brockman Iron Formation|24047|6|Mentioned|p19|||||||||
2602|Brockman Iron Formation|24168|5|Briefly described|p632|||||||||
2602|Brockman Iron Formation|24231|5|Briefly described|p185, p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
2602|Brockman Iron Formation|24426|5|Briefly described|p216 Fig.1|Paleoproterozoic|Archean|Of Hamersley Group. Geological Province: Hamersley Province.||||||07-FEB-11
2602|Brockman Iron Formation|24541|3|Fully described|p2, p11 Tb.2, p57|Paleoproterozoic|Neoarchean|Age: c. 2490 Ma. Overlain by Weeli Wolli Formation. Of the Hamersley Group. Maximum Thickness: 600m.||||||09-DEC-08
2602|Brockman Iron Formation|24543|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group (Mount Bruce Supergroup).  Banded iron formation and minor siltstone.  Age: c.2490Ma.||||||23-DEC-09
2602|Brockman Iron Formation|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Hamersley Group. Overlies Mount McRae Shale. Overlain by Weeli Wolli Formation. Banded iron-formation. Geological Province: Hamersley Basin.||||||07-NOV-08
2602|Brockman Iron Formation|24573|5|Briefly described|p671 Fig.2|Proterozoic|Proterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton||||||
2602|Brockman Iron Formation|29586|6|Mentioned|p23|||||||||
2602|Brockman Iron Formation|29594|6|Mentioned|p9|||||||||
2602|Brockman Iron Formation|29595|6|Mentioned|Fig.2|||||||||
2602|Brockman Iron Formation|29596|6|Mentioned|Fig.2|||||||||
2602|Brockman Iron Formation|29629|5|Briefly described|p899|||||||||
2602|Brockman Iron Formation|29715|6|Mentioned|p33|||||||||
2602|Brockman Iron Formation|29716|4|Described|Table 1|||||||||
2602|Brockman Iron Formation|29717|6|Mentioned|p1153|||||||||
2602|Brockman Iron Formation|29848|6|Mentioned|p414|||||||||
2602|Brockman Iron Formation|30437|6|Mentioned|p89|||Bulk of hematite deposits||||||
2602|Brockman Iron Formation|30488|6|Mentioned|p88|||Abundant tourmaline. Source of boron. Refers Trendall & Blackley (1970)||||||
2602|Brockman Iron Formation|30685|5|Briefly described|p907|||Re mineralization||||||
2602|Brockman Iron Formation|31021|5|Briefly described|p893|||||||||
2602|Brockman Iron Formation|31670|4|Described|p912|||||||||
2602|Brockman Iron Formation|31671|4|Described|p11|||||||||
2602|Brockman Iron Formation|31828|6|Mentioned|p41|||Asbestos. See also P32 - banded iron formation||||||
2602|Brockman Iron Formation|31931|6|Mentioned|p81|||||||||
2602|Brockman Iron Formation|32144|6|Mentioned|p85|||Organic activity, genesis||||||
2602|Brockman Iron Formation|32326|6|Mentioned|p122|||Hamersley Group.||||||
2602|Brockman Iron Formation|32389|6|Mentioned|p924|||||||||
2602|Brockman Iron Formation|32792|6|Mentioned|p257|||||||||
2602|Brockman Iron Formation|33538|6|Mentioned|p291|||||||||
2602|Brockman Iron Formation|33540|6|Mentioned|p884|||||||||
2602|Brockman Iron Formation|33542|6|Mentioned|p412|||||||||
2602|Brockman Iron Formation|33544|4|Described|p41|||See also pp42 - 80.||||||23-OCT-15
2602|Brockman Iron Formation|33545|5|Briefly described|p112|||||||||
2602|Brockman Iron Formation|33687|5|Briefly described|p917|||||||||
2602|Brockman Iron Formation|34023|6|Mentioned|p46|||||||||
2602|Brockman Iron Formation|34066|4|Described|p5|||L.Prot. See also p6.||||||17-SEP-18
2602|Brockman Iron Formation|34115|6|Mentioned|p383|||||||||
2602|Brockman Iron Formation|34135|4|Described|Table 1|||Lower Proterozoic. See also pp5,7,12,13 etc.||||||17-SEP-18
2602|Brockman Iron Formation|34203|6|Mentioned|p15|||||||||
2602|Brockman Iron Formation|34287|6|Mentioned|p55|||Hamersley Group||||||
2602|Brockman Iron Formation|34541|6|Mentioned|p53|||||||||
2602|Brockman Iron Formation|34542|6|Mentioned|p94|||||||||
2602|Brockman Iron Formation|34887|6|Mentioned|p19|||||||||
2602|Brockman Iron Formation|35052|6|Mentioned|Fig.2|||||||||
2602|Brockman Iron Formation|35056|6|Mentioned|p90|||||||||
2602|Brockman Iron Formation|35218|6|Mentioned|Fig.1|||||||||
2602|Brockman Iron Formation|35260|6|Mentioned|Fig.4|||||||||
2602|Brockman Iron Formation|35269|6|Mentioned|p309|||||||||
2602|Brockman Iron Formation|35299|5|Briefly described|p893|||||||||
2602|Brockman Iron Formation|35976|6|Mentioned|Fig.39|||||||||
2602|Brockman Iron Formation|35977|6|Mentioned|p115|||||||||
2602|Brockman Iron Formation|36003|6|Mentioned|p1032|||||||||
2602|Brockman Iron Formation|36004|6|Mentioned|p1089|||||||||
2602|Brockman Iron Formation|36091|4|Described|p572|||||||||
2602|Brockman Iron Formation|36247|6|Mentioned|p185|||See also Fig.2.||||||
2602|Brockman Iron Formation|36260|5|Briefly described|p78|Paleoproterozoic|Paleoproterozoic|Comprises Dales Gorge, Whaleback Shale, Joffre and Yandicoogina Shale Members. Geological Province: Hamersley Basin. banded iron formation.||||||07-NOV-08
2602|Brockman Iron Formation|36362|6|Mentioned|Fig.5|||||||||
2602|Brockman Iron Formation|36551|6|Mentioned|Table 23|||||||||
2602|Brockman Iron Formation|36642|6|Mentioned|Table 1|||||||||
2602|Brockman Iron Formation|36882|4|Described|p132|||||||||
2602|Brockman Iron Formation|36891|5|Briefly described|p441|||||||||
2602|Brockman Iron Formation|37170|5|Briefly described|p195|||||||||
2602|Brockman Iron Formation|37226|6|Mentioned|Fig.1|||||||||
2602|Brockman Iron Formation|37297|6|Mentioned|p96|||||||||
2602|Brockman Iron Formation|37352|6|Mentioned|p96|||||||||
2602|Brockman Iron Formation|37371|6|Mentioned|p366|||||||||
2602|Brockman Iron Formation|37460|6|Mentioned|Fig.3.4|||||||||
2602|Brockman Iron Formation|37577|6|Mentioned|p30|||||||||
2602|Brockman Iron Formation|37704|6|Mentioned|Fig.1|||||||||
2602|Brockman Iron Formation|37708|6|Mentioned|p1929|||||||||
2602|Brockman Iron Formation|37709|6|Mentioned|p1969|||||||||
2602|Brockman Iron Formation|38102|6|Mentioned|p189|||||||||
2602|Brockman Iron Formation|38790|6|Mentioned|p164|||||||||
2602|Brockman Iron Formation|39200|6|Mentioned|p286|||||||||
2602|Brockman Iron Formation|39210|5|Briefly described|Table 1|||||||||
2602|Brockman Iron Formation|39558|6|Mentioned|Table 1|||||||||
2602|Brockman Iron Formation|39589|6|Mentioned|p157|||||||||
2602|Brockman Iron Formation|39697|5|Briefly described|p126|||||||||
2602|Brockman Iron Formation|40369|6|Mentioned|Plate 1|||||||||
2602|Brockman Iron Formation|40537|6|Mentioned|p349|||||||||
2602|Brockman Iron Formation|40790|6|Mentioned|p192|||||||||
2602|Brockman Iron Formation|40852|5|Briefly described|p23|||||||||
2602|Brockman Iron Formation|40854|6|Mentioned|p365|||||||||
2602|Brockman Iron Formation|41358|5|Briefly described|p145|||||||||
2602|Brockman Iron Formation|41622|6|Mentioned|p272|||||||||
2602|Brockman Iron Formation|41635|6|Mentioned|p19|||||||||
2602|Brockman Iron Formation|41768|5|Briefly described|Table 1|||See also P28||||||
2602|Brockman Iron Formation|41846|6|Mentioned|p97|||||||||
2602|Brockman Iron Formation|41847|6|Mentioned|p107|||||||||
2602|Brockman Iron Formation|42013|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
2602|Brockman Iron Formation|42112|5|Briefly described|p9|||||||||
2602|Brockman Iron Formation|42148|6|Mentioned|p690|||||||||
2602|Brockman Iron Formation|42190|6|Mentioned|p274|||||||||
2602|Brockman Iron Formation|42260|6|Mentioned|p42|||||||||
2602|Brockman Iron Formation|42471|5|Briefly described|p8|||||||||
2602|Brockman Iron Formation|42472|5|Briefly described|Map legend|||||||||23-DEC-09
2602|Brockman Iron Formation|42495|6|Mentioned|p2|||||||||
2602|Brockman Iron Formation|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
2602|Brockman Iron Formation|42704|5|Briefly described|Plate 2E|Proterozoic|Archean|Of the Hamersley Group.  banded-iron formation, chert, shale. Age: ~2500Ma.||||||07-NOV-08
2602|Brockman Iron Formation|42730|6|Mentioned|p12|||||||||
2602|Brockman Iron Formation|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
2602|Brockman Iron Formation|42744|5|Briefly described|p5|||||||||
2602|Brockman Iron Formation|42785|6|Mentioned|p262|||of Hamersley Group.||||||
2602|Brockman Iron Formation|43052|6|Mentioned|p68|||||||||
2602|Brockman Iron Formation|43063|6|Mentioned|p49|||||||||
2602|Brockman Iron Formation|43119|5|Briefly described|p10|||of Hamersley Group||||||
2602|Brockman Iron Formation|43210|5|Briefly described|Table 1 p3,p4.||Mesoproterozoic|of Hamersley Group.||||||
2602|Brockman Iron Formation|43262|5|Briefly described|Map Legend||Proterozoic|of Hamersley Group.||||||
2602|Brockman Iron Formation|43290|5|Briefly described|p6||Proterozoic|of Hamersley Group.||||||
2602|Brockman Iron Formation|43644|6|Mentioned|p594|||||||||
2602|Brockman Iron Formation|43673|6|Mentioned|p374|||||||||
2602|Brockman Iron Formation|44152|5|Briefly described|p164, p178-180, p182, p185 Tb.2-25|||||Hamersley Group.|Includes Dales Gorge Member; Whaleback and Yandicoogina, Shale Members; Joffre Member.|Overlies Mount McRae Shale. Is overlain by Weeli Wolli Formation.|BIF, shale.|
2602|Brockman Iron Formation|44438|14|Not recorded|map legend||Paleoproterozoic|Formation of Hamersley Group. L.Proterozoic.||||||07-NOV-08
2602|Brockman Iron Formation|44477|4|Described|p.11, Table 1||Proterozoic|SF/50-6.||||||
2602|Brockman Iron Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
2602|Brockman Iron Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
2602|Brockman Iron Formation|44491|14|Not recorded|map legend|||Correlation.||||||
2602|Brockman Iron Formation|44492|14|Not recorded|p.8,opp.p.5, map||Proterozoic|(F50-1,2).||||||
2602|Brockman Iron Formation|44501|4|Described|p.6,19,20,Tb.4, map||Paleoproterozoic|Lower Proterozoic. p.27,30. (ref. to MacLeod et al 1963). (F/50-7).||||||07-NOV-08
2602|Brockman Iron Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
2602|Brockman Iron Formation|44503|2|Defined|p.14,15,Tb.2, map|||See also p.5,17,18,20,22-24, for more details. Roy Hill Sheet (F50-12).||||||
2602|Brockman Iron Formation|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
2602|Brockman Iron Formation|44692|2|Defined|p.7,12-15,,Tb.1|||See also p. 19,22,24, for more details. (F50-11).||||||
2602|Brockman Iron Formation|44729|5|Briefly described|map legend|Proterozoic||Of Hamersley Group||||||
2602|Brockman Iron Formation|46899|6|Mentioned|p8|||Heat flow||||||
2602|Brockman Iron Formation|48755|6|Mentioned|p12|||||||||
2602|Brockman Iron Formation|48760|6|Mentioned|p125|||||||||
2602|Brockman Iron Formation|50227|5|Briefly described|p442, p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group.  Geological Province: Hamersley Province.  See also p447 Fig. 3.||||||07-FEB-11
2602|Brockman Iron Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Hamersley Group. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
2602|Brockman Iron Formation|50549|6|Mentioned|p1159|||||||||
2602|Brockman Iron Formation|60373|5|Briefly described|p145 Tb. 1|Archean|Archean|Of Hamersly Group. Includes Dales Gorge, Whaleback Shale, Joffre and Yandicoogina Shale Members. Overlian by Weeli Wolli Formation, underlain by Mount McRae Shale.||||||
2602|Brockman Iron Formation|60706|5|Briefly described|p623, p631, p643 App.1|Paleoproterozoic|Archean|Of the Hamersley Group. Includes Dales Gorge, Whaleback Shale, Joffre and Yandicoogina Shale Members. Geological Province: Hamersley Bsin.|2495+/-5 Ma (SHRIMP) - 2451 Ma inferred.|||||06-OCT-15
2602|Brockman Iron Formation|61265|5|Briefly described|p46-47 Fig.2|||Of the Hamersley Group. Geological Province: Pilbara Craton.||||||
2602|Brockman Iron Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Hamersley Group. Banded-iron formation, chert, mudstone, and siltstone.||||||
2602|Brockman Iron Formation|61560|5|Briefly described|p498 Tb. 4|||Includes the Dales Gorge Member. Geological Province: Hamersley Basin.||||||
2602|Brockman Iron Formation|61575|5|Briefly described|p760 Fig. 2|||||||||
2602|Brockman Iron Formation|61576|5|Briefly described|p774 Fig. 1|Paleoproterozoic||Of the Hamersley Group. Age: ~2469+/-3Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
2602|Brockman Iron Formation|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
2602|Brockman Iron Formation|61847|5|Briefly described|p295 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Pilbara Craton.||||||07-NOV-08
2602|Brockman Iron Formation|62129|3|Fully described|p2, p10, p21, p24|Archaean|Archaean|Of the Hamersley Group. Includes Dales George, Whaleback Shale, Joffre and Yandicoogina Shale Members. Thickness: 550m. Geological Province: Hamersley Basin.||||||02-MAR-15
2602|Brockman Iron Formation|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Hamersley Group. Age: c. 2490Ma. Geological Province: Hamersley Basin, Pilbara Craton. Banded iron-formation, chert, and pelite.||||||23-DEC-09
2602|Brockman Iron Formation|63153|6|Mentioned|p1359, p1362 Fig.3, p1363, p1368, p1370|||Hosts subsidiary deposits of the Hope Downs high-grade hematite ore deposit. Appears as Brockman Formation on p1368 and p1370.||Unit in Hamersley Group.|Includes Dales Gorge, Whaleback Shale, Joffre, Yandicoogina Shale, Members.|Overlies Mount McRae Shale. Is overlain by Weeli Wolli Formation.||
2602|Brockman Iron Formation|63236|5|Briefly described|Map legend|||Mapping also includes some Weeli Wolli Formation. Geological Province: Hammersley Basin. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||16-JAN-08
2602|Brockman Iron Formation|63372|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hamersley Group. Geological Province: Hamersley Basin. Age: 2479-2454Ma. Banded iron formation, chert, mudstone and siltstone. Underlies: Weeli Wolli Formation. Overlies: Mount McRae Shale and Mount Sylvia Formation.||||||23-DEC-09
2602|Brockman Iron Formation|63432|5|Briefly described|p736 Fig. 2 and Fig. 3|Proterozoic|Proterozoic|BIF/shales unit.||||||07-FEB-11
2602|Brockman Iron Formation|64384|5|Briefly described|p35 Tb. 6, p36|||Of Hamersley Group. Comprises 4 members: Dales Gorge Member. Geol.prov: Hamersley Basin. The thickest and most important BIF in the group.||||||07-FEB-11
2602|Brockman Iron Formation|64406|5|Briefly described|p1-2|||Contains the Yandicoogina Shale, Joffre, Whaleback Shale and Dales Gorge Members. Geological Province: Hamersley Basin.  Discussed in the context of its use as facing stone forming the lift panels in Mineral House, Perth.||||||
2602|Brockman Iron Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Upper Hamersley Group. Banded iron-formation, chert, mudstone, and siltstone; metamorphosed.||||||09-DEC-08
2602|Brockman Iron Formation|64688|5|Briefly described|Map legend|Archaean|Archaean|Geological province: Hamersley Basin. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||
2602|Brockman Iron Formation|64724|5|Briefly described|p43, p42 Fig. 3|Paleoproterozoic|Paleoproterozoic|Sediments of the Hamersley Basin deposited (along with overlying Hamersley Group units) in a convergent continental back-arc basin setting between ~2470 and ~2450 Ma.||Of Hamersley Group.||||02-APR-12
2602|Brockman Iron Formation|65683|5|Briefly described|p799, p801 Fig2,|||Of Hamersley Group. Includes Dales Gorge and Joffre Members, Whaleback Shale and Yandicoogina Shale Members.||||||08-MAR-12
2602|Brockman Iron Formation|65757|5|Briefly described|p81 Tb.2, p84 Fig.2, p88|||Includes Dales Gorge Member, Mount Whaleback Member,Joffre Member, Yandicoogina Member. Part of the Hamersley Group. Overlain by Weeli Wolli Formation.||||||06-OCT-15
2602|Brockman Iron Formation|66574|6|Mentioned|p920 Fig.9|||Unit in Hamersley Group.||||||
2602|Brockman Iron Formation|66882|5|Briefly described|p118|Siderian|Neoarchean|Contains the majority of main iron ore zones.|c.2500-2460 Ma|Hamersley Group.|||BIF.|
2602|Brockman Iron Formation|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.|~2470-~2450 Ma estimated from Fig.11.|||||
2602|Brockman Iron Formation|67025|4|Described|pp318-328.|||620 m thick. Contains much of the iron ore deposits in the Hamersley Group. The natural remanent magnetisation and mean bulk susceptibility of this unit are discussed in this article.||Unit in Hamersley Group.|Comprises Dales Gorge, Whaleback Shale, Joffre, and Yandicoogina Shale Members.|Conformably overlies Mount McRae Shale. Is overlain conformably by Weeli Wolli Formation.||
2602|Brockman Iron Formation|67056|4|Described|p418 Fig.1, p419 Fig.2, p420 Fig.3(a).|||Hamersley Province. Various occurrences in the Ophthalmia Ranges and the Brockman Syncline. Tonnage per strike km ranges from 35 to 350 Mt and appears to be affected by folding.||Unit in Hamersley Group.|Includes Dales Gorge and Joffre Members; Mount Whaleback and Yandicoogina Shales.|Is overlain by Weeli Wolli Formation.||
2602|Brockman Iron Formation|67130|5|Briefly described|p1, p8, p24 fig 17, p39 fig 36, p41-42|Siderian|Siderian||2475 Ma -2463 Ma|Hamersley Group|Includes Dales Gorge Member, Whaleback Shale Member, Joffre Member, Yandicoogina Shale Member|Overlies Mount McRae Shale, overlain by Woongarra Rhyolite|Banded iron formation|
2602|Brockman Iron Formation|67183|6|Mentioned|p643, p645 Tb.1|Archean|Archean|Present in the Southern Pilbara. Neoarchean?||Hamersley Group||Apparent lateral equivalent to the Carawine Dolomite.||
2602|Brockman Iron Formation|67201|4|Described|p32, p34, p51-55|||Visible at base of Hamersley Range Escarpment. Thickness: 610 m section, over 40 m.y.|members incl c.2495,c.2463,c.2454 Ma SHRIMP U-Pb|Hamersley Group||Overlain Weeli Wooli Formation. Overlies Wittenoom Formation, Mount Sylvia Formation and Mount McRae Shale, and Jeerinah Formation.|BIF-dominated.|22-NOV-16
2602|Brockman Iron Formation|67827|6|Mentioned|p411, p414 Fig.4, p415, p416 Fig.5 |||Hamersley Province. Microstructure of iron ores discussed.|||Includes Joffre Member.|||
2602|Brockman Iron Formation|67855|6|Mentioned|p226, 227, 228||||||Includes Dales Gorge Member, Joffre Member.|||
2602|Brockman Iron Formation|68035|5|Briefly described|p292, Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Of Hamersley Group.|Includes Dales Gorge Member, Whaleback Shale Member, Joffre Member, Yandicoogina Shale Member.|Overlies Mount McRae Shale, overlain by Weeli Wolli Formation.|BIF-dominated.|
2602|Brockman Iron Formation|68280|5|Briefly described|p1, p5, p41, p54, p62|Paleoproterozoic|Paleoproterozoic||2490-2460 Ma|Hamersley Group|Includes Yandicoogina Shale Member, Joffre Member, Whaleback Shale Member, Dales Gorge Member|Overlain by Weeli Wolli Formation, overlies Mount McRae Shale|610m thick. Alternating shale and banded iron formation in macrobands.|
2602|Brockman Iron Formation|69028|5|Briefly described|Map Legend|||Hamersley Basin.||Of the Hamersley Group.|||Banded iron-formation, chert, mudstone and siltstone; metamorphosed.|07-MAY-14
2602|Brockman Iron Formation|69080|6|Mentioned|p687|||||Unit in Hamersley Group.||Overlies Mount McRae Shale. Is overlain by Weeli Wolli Formation.||
2602|Brockman Iron Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Hamersley Group|||Banded iron-formation, chert, mudstone, and siltstone; metamorphosed.|
2602|Brockman Iron Formation|69185|5|Briefly described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2490 Ma|Unit of Hamersley Group.|||Banded iron-formation, chert, mudstone, and siltstone; metamorphosed|
2602|Brockman Iron Formation|69538|5|Briefly described|p513-586|Paleoproterozoic|Paleoproterozoic|Main source of DID (detrital iron deposits) from eroded ferruginised surface BIF.||Unit in Hamersley Group.|Includes Dales Gorge, Whaleback Shale, Joffre, and Yandicoogina Shale, Members.|||
2602|Brockman Iron Formation|69563|5|Briefly described|p689-690||||2481 +/- 4 Ma.|Unit in Hamersley Group.|Includes Dales Gorge, Whaleback Shale, and Joffre, Members.|||
2602|Brockman Iron Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Hamersley Group.||||
2602|Brockman Iron Formation|69590|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|Of Hamersley Basin. Events: Paterson Orogeny; Miles Orogeny.||Unit of Hamersley Group.|||Banded iron-formation, chert, mudstone, and siltstone; metamorphosed|
2602|Brockman Iron Formation|69739|5|Briefly described|p69-71|||Hamersley Basin.||Hamersley Group.||Overlies Mount McRae Shale.|Iron-oxide dominated. Water-bearing.|
2602|Brockman Iron Formation|69745|6|Mentioned|p268-269, 272-274, 276-279, 281-284|Proterozoic|Proterozoic|Crops out in the Mount Wall Fe deposit area, Hamersley Province. See also p286-288, 290.||Hamersley Group.|Yandicoogina Shale, Dales Gorge, Joffre, Whaleback Shale Members.|||
2602|Brockman Iron Formation|69754|6|Mentioned|p331|||Pilbara Craton.||Hamersley Group||||
2602|Brockman Iron Formation|70509|5|Briefly described|p12-14,21,32|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. Thickness: ~620m. ||Unit of Hamersley Group.|Includes Yandicoogina Shale Member, Joffre Member, Whaleback Shale Member and Dales Gorge Member.|Overlain by Weeli Wolli Formation. Underlain by Mount McRae Shale.||
2602|Brockman Iron Formation|70775|6|Mentioned|p2|||||Hamersley Group||||
2602|Brockman Iron Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Hamersley Basin|2494-2451 Ma||||Banded iron formation, chert, mudstone and siltstone; metamorphosed.|
2602|Brockman Iron Formation|71042|5|Briefly described|p65, p69|Paleoproterozoic|Paleoproterozoic|||Hamersley Group||Equivalent to the Carawine Dolomite.|Banded iron formation.|
2602|Brockman Iron Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||chert, mudstone, siltstone, banded iron formation|
2602|Brockman Iron Formation|71513|5|Briefly described|p65-69, p71, p73, p75, p77-82, p86-88|||Pilbara Craton. Interpreted to have been deposited in a back-arc setting. Magnetite in this formation was interpreted to be derived from oxidation of primary ferrous iron minerals.||Hamersley Group.|Includes the Dales Gorge Member, Joffre Member and the Whaleback Shale Member.|Overlies the Mt Sylvia and Mt McRae shales.|Banded-iron formation.|
2602|Brockman Iron Formation|71785|14|Not recorded|p86-91|||Of Hamersley Group.||||||
2602|Brockman Iron Formation|71808|5|Briefly described|v, ix, p2, p6, p10, p30, p40, p44|||Hamersley Province. This unit can be readily interpreted on a regional scale in aerial photos. See also p47, p53, p65, p83, p107, p117, p135, p149-p150, p156.||Hamersley Group|Includes the Mount Whaleback Shale Member.|||
2602|Brockman Iron Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Hamersley Basin.||Hamersley Group, upper|||Banded iron-formation, chert, mudstone, and siltstone; metamorphosed.|
2602|Brockman Iron Formation|72254|6|Mentioned|App.A p10-11|||Pilbara Craton.||Hamersley Group, Mount Bruce Supergroup|Joffre Member|||
2602|Brockman Iron Formation|72493|5|Briefly described|p27-30, 44|Palaeoproterozoic|Palaeoproterozoic|Hamersley Basin. 620m thick.|||Dales Gorge, Whaleback Shale, Joffre, Members.|||
2602|Brockman Iron Formation|72569|6|Mentioned|p2|||Of the Hamersley Basin.|||Includes the Dales Gorge Member.|||
2602|Brockman Iron Formation|72570|6|Mentioned|p3 fig 1|||||Hamersley Group||||
2602|Brockman Iron Formation|72712|5|Briefly described|p7, p9, p10-11, p44, p54.|Siderian|Siderian|See also p55 Fig.36. This formation is well exposed in a creek section along the Beasley River at Woongarra Pool.|c. 2495 Ma to c. 2460 Ma.|Hamersley Group|Dales Gorge, Whaleback Shale, Joffre and the Yandicoogina Shale Members.|Overlies Mount McRae Shale and conformably underlies Weeli Wolli Formation.||14-JAN-21
2602|Brockman Iron Formation|72758|5|Briefly described|p15 Tb.1, p23, p25, p33, p55.|Paleoproterozoic||650m thick. The constituent members are present over much of northeastern Wyloo.||Hamersley Group|Dales Gorge Member, Whaleback Shale Member, Joffre Member, Yandicoogina Shale Member|Conformably overlies Mount McRae Shale and conformably underlies Weeli Wooli Formation.|Banded iron formation and mudstone.|
2602|Brockman Iron Formation|73022|4|Described|p1-2, p3 Fig.2, p4 Fig.3, p5-7|Siderian|Siderian|BIF sequences deposited in association with basin drowning.|2.49, 2.48 Ga|Hamersley Group|Dales Gorge Member, Whaleback Shale Member, Joffre Member, Yandicoogina Shale Member.|Overlies the Mount McRae Shale and Colonial Chert Member, underlies the Weeli Wolli Formation.|Banded iron formation, includes lesser shale and minor Fe-chert.|
2602|Brockman Iron Formation|73290|6|Mentioned|p783||||||Dales Gorge Member.|||
2602|Brockman Iron Formation|73538|6|Mentioned|p4|||||Hamersley Group|Yandicoogina Shale Member, Joffre Member, Whaleback Shale, Dales Gorge Member|Underlain by McRae Shale. Overlain by Weeli Wolli Formation.|Includes mudstone/siltstone and iron formation.|
2602|Brockman Iron Formation|73574|6|Mentioned|p770, p771 Fig.6||||||||Banded iron Formation.|
2608|Brodagee Sandstone|22484|5|Briefly described|p83 Fig13|||of the Mount Minnie Group||||||
2608|Brodagee Sandstone|23325|5|Briefly described|map legend|Proterozoic|Proterozoic|of Mount Minnie Group||||||
2608|Brodagee Sandstone|24544|4|Described|p48|Paleoproterozoic|Paleoproterozoic|Of Mount Minnie Group. Quartz sandstone, conglomerate. Geological Province: Ashburton Province.||||||07-NOV-08
2608|Brodagee Sandstone|34066|4|Described|p9|||Mid. Prot.||||||
2608|Brodagee Sandstone|36883|3|Fully described|p145|||||||||
2608|Brodagee Sandstone|42260|4|Described|p98|||||||||
2608|Brodagee Sandstone|44477|6|Mentioned|p.12||Proterozoic|SF/50-6.||||||
2608|Brodagee Sandstone|44481|5|Briefly described|map legend||Mesoproterozoic|||||||
2608|Brodagee Sandstone|67855|5|Briefly described|p221|||750m thick.||Mount Minnie Group||Overlain by Wabco Shale (conformably).|Thick-bedded cross-stratified sandstone and conglomerate containing rounded clasts of quartz sandstone, chert, vein quartz and jaspilite plus mudstone fragments from Ashburton Formation.|
2608|Brodagee Sandstone|69028|5|Briefly described|Map Legend|Statherian|Statherian|Ashburton and Blair Basins. Mapped with Wabco Shale and Warramboo Sandstone as a single unit.||Of the Mount Minnie Group.|||Quartz sandstone, conglomerate, siltstone, and mudstone.|07-MAY-14
2608|Brodagee Sandstone|72758|5|Briefly described|p10 Tb.1, p48-49.|||750 m thick. Fluvial with localized alluvial fan deposits.||Mount Minnie Group||Unconformably overlies Ashburton Formation and underlies Wabco Shale.|Silicified, thick-bedded sandstone with laterally restricted basal conglomerate with sandstones often occuring in upward fining sets, pebbly at base, with trough cross stratification.|
2625|Bronzite Complex|32092|6|Mentioned|p130|||||||||
2645|Broome Sandstone|7433|4|Described|p25 Fig.2, p42, pp44-45, p52.|Cretaceous|Cretaceous|Canning Basin. Shallow marine-tidal clastics. Up to 274 m thick. Contains plant fossils and rare bivalves; alternating traction current and suspension deposits; scour-and-fill, rippled sandstone and mudstone drapes. Excellent fresh-water aquifer.|||Includes Jowlaenga Formation and Leveque Sandstone.|Overlies Jarlemai Siltstone. Is overlain by Melligo Sandstone. Is disconformably overlain by Parda Formation, Frezier Sandstone, and by Emeriau Sandstone in the far north of the basin.|Sandstone, minor mudstone.|
2645|Broome Sandstone|13255|6|Mentioned|p369|Early Cretaceous|Early Cretaceous|Roebuck Basin.||||Overlies Egret Formation. Is overlain by Mermaid Formation.||
2645|Broome Sandstone|22717|6|Mentioned|p13||Early Cretaceous|||||||14-APR-20
2645|Broome Sandstone|22718|5|Briefly described|P4, P8, Table1||Early Cretaceous|||||||
2645|Broome Sandstone|22738|4|Described|9,13,14,16,17, map|Early Cretaceous|Early Cretaceous|Max thickness 265 m. Overlain by Parda Formation; underlain by Jarlemai Siltstone.||||||13-NOV-07
2645|Broome Sandstone|22753|5|Briefly described|Fig.3 p585|Cretaceous|Cretaceous|||||||
2645|Broome Sandstone|22765|5|Briefly described|P6, P10, Table1|Early Cretaceous|Late Jurassic|Maximum thickness of 192m, Overlies Jarlemai Siltstone and underlies Melligo Sandstone||||||
2645|Broome Sandstone|22767|5|Briefly described|Table3 P12, P23||Early Cretaceous|||||||
2645|Broome Sandstone|22801|6|Mentioned|P13|||||||||
2645|Broome Sandstone|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
2645|Broome Sandstone|23212|4|Described|Table.1 p11||Neocomian|Partly equivalent to Mowla Sandstone.||||||
2645|Broome Sandstone|23722|6|Mentioned|p35|Cretaceous|Cretaceous|||||||
2645|Broome Sandstone|23765|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||23-DEC-09
2645|Broome Sandstone|23766|4|Described|p13 Tb. 2|Early Cretaceous|Late Jurassic|Consists of fine to coarse sandstone with conglomerate near the base. Thickness: 254m. See also p29.||||||01-JUL-08
2645|Broome Sandstone|24061|5|Briefly described|p183|Early Cretaceous|Early Cretaceous|Geological Province:  Canning Basin.||||||
2645|Broome Sandstone|24062|5|Briefly described|p186 Table 1|Cretaceous|Jurassic|Geological Province: Canning Basin.||||||
2645|Broome Sandstone|24449|6|Mentioned|p744|||Geological Province: Canning Basin.||||||
2645|Broome Sandstone|29693|6|Mentioned|p35|||||||||
2645|Broome Sandstone|30110|6|Mentioned|p81|||Neocomian - Aptian age. Part of Winning Group.||||||
2645|Broome Sandstone|30313|6|Mentioned|p54|||||||||
2645|Broome Sandstone|32024|6|Mentioned|p13|||Cretaceous||||||
2645|Broome Sandstone|32025|6|Mentioned|p978|||Major exploration target||||||
2645|Broome Sandstone|32648|6|Mentioned|p32|||L.Cret.||||||
2645|Broome Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
2645|Broome Sandstone|33939|6|Mentioned|p393|||Flora. U.Jur. - L.Cret.||||||
2645|Broome Sandstone|34363|6|Mentioned|p56|||Neocomian. See Fig.7.||||||
2645|Broome Sandstone|34548|6|Mentioned|p131|||Lower Cretaceous||||||
2645|Broome Sandstone|35275|6|Mentioned|Fig.5.|||||||||
2645|Broome Sandstone|35711|4|Described|p27|||See also Table 3,stratigraphy. Hydrogeology on p37..||||||13-NOV-07
2645|Broome Sandstone|35969|6|Mentioned|p66|||Hydrogeology discussed P70.||||||
2645|Broome Sandstone|36257|6|Mentioned|Table 2.1|||||||||
2645|Broome Sandstone|36634|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|36890|3|Fully described|p351|||Formerly Broome Beds.||||||01-OCT-08
2645|Broome Sandstone|37368|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|37369|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|37370|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|38878|6|Mentioned|Map legend|Aptian|Tithonian|Tithonian - Aptian||||||
2645|Broome Sandstone|38886|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|39857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|40045|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|40078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
2645|Broome Sandstone|40992|6|Mentioned|Fig.11|||||||||
2645|Broome Sandstone|41169|6|Mentioned|Fig.3|||||||||
2645|Broome Sandstone|41730|6|Mentioned|Fig.3|||||||||
2645|Broome Sandstone|42338|5|Briefly described|Table 1 P145|||||||||
2645|Broome Sandstone|42473|6|Mentioned|p93|||||||||
2645|Broome Sandstone|42477|5|Briefly described|p155|||||||||
2645|Broome Sandstone|42571|4|Described|p13|||Cretaceous||||||
2645|Broome Sandstone|42572|5|Briefly described|Map Legend|Cretaceous||||||||23-DEC-09
2645|Broome Sandstone|42734|5|Briefly described|map legend|Cretaceous||||||||
2645|Broome Sandstone|42792|5|Briefly described|Table 1 P225|||||||||
2645|Broome Sandstone|42814|5|Briefly described|p24|||||||||
2645|Broome Sandstone|42930|5|Briefly described|Fig.1 p473|Cretaceous|Cretaceous|Unconformable over Jarlemai Siltstone. Geological Province: Canning Basin. Deltaic deposits.||||||13-NOV-07
2645|Broome Sandstone|43173|6|Mentioned|13|Early Cretaceous|Late Jurassic|||||||
2645|Broome Sandstone|43307|5|Briefly described|Map Legend||Cretaceous|||||||
2645|Broome Sandstone|43563|6|Mentioned|Fig.2,p5||Early Cretaceous|||||||
2645|Broome Sandstone|43656|6|Mentioned|Fig.2,p8|Barremian|Berriasian|||||||
2645|Broome Sandstone|43666|6|Mentioned|p45,Table 2|Valanginian|Berriasian|||||||
2645|Broome Sandstone|43746|6|Mentioned|Fig.2,p11|Barremian|Berriasian|||||||
2645|Broome Sandstone|43818|6|Mentioned|Fig.2.p39||Early Cretaceous|||||||
2645|Broome Sandstone|44040|14|Not recorded|p43|||||||||
2645|Broome Sandstone|44143|4|Described|p.431 Table 4-19; p.449-450|Cretaceous|Jurassic|274m thick in Tappers Inlet 1; fine to coarse sandstone, mudstone; shallow marine (tidal). Conformably(?) overlies the Jarlemai Siltstone; is overlain conformably by Melligo Sandstone and disconformably by Parda Formation, Emeriau and Frezier Sandstones. Onshore facies equivalent of Mermaid Formation. Type section at Gantheaume Point (BROOME: 17deg 58' 30" S, 122deg 10' 30" E). Contains dinosaur footprints in Broome area.||||||22-NOV-17
2645|Broome Sandstone|44357|4|Described|p14,Tb.1 p8||Early Cretaceous|||||||
2645|Broome Sandstone|44997|14|Not recorded|p.25,38||Neocomian|||||||
2645|Broome Sandstone|44998|2|Defined|p.179|||Overlies "Broome Buchia Beds". Overlain by Leveque Sandstone. On many pages. p.119,133,146,152,162,182,185,196. See also App.6 p291,296,297.||||||
2645|Broome Sandstone|45011|14|Not recorded|p64,71,72||Neocomian|||||||
2645|Broome Sandstone|45153|2|Defined|App.8-131|late Neocomian|late Neocomian|See also App.6-95, App.6-112.||||||
2645|Broome Sandstone|45158|3|Fully described|p14|||See also p13.||||||13-NOV-07
2645|Broome Sandstone|45168|6|Mentioned|p6|||||||||
2645|Broome Sandstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
2645|Broome Sandstone|61021|5|Briefly described|p36 Fig. 2|Hauterivian|Berriasian|Geological Province: Canning Basin.||||||17-DEC-07
2645|Broome Sandstone|64186|5|Briefly described|p171, p170 Fig. 1|Neocomian|Neocomian|Upper most unit of the Broome Platform. Max thickness: 266m.||||||
2645|Broome Sandstone|64449|5|Briefly described|p62 Tb. 2|Early Cretaceous|Early Cretaceous|Consists of cross-bedded, bedded to laminated, fine to very coarse sandstone, mudstone and minor conglomerate.||||||07-FEB-11
2645|Broome Sandstone|64580|4|Described|map legend||Early Cretaceous|Fine- to coarse-grained sandstone; minor mudstone and conglomerate.||||||09-DEC-08
2645|Broome Sandstone|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
2645|Broome Sandstone|64982|6|Mentioned|p700.|||||||||
2645|Broome Sandstone|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||23-FEB-10
2645|Broome Sandstone|65449|5|Briefly described|p6|Early Cretaceous|Early Cretaceous|||||Unconformably overlies Jarlemai Siltstone. Lateral equivalent of Callawa and Cronin Formations. Is overlain by Frezier and Melligo Sandstones and Parda Formation.||
2645|Broome Sandstone|65553|5|Briefly described|p1-2, Fig 2-6||Cretaceous|Exposed as rock pavements at James Price Point 60 km north of Broome. Contains dinosaur (sauropod) foot prints and body impressions.|~130 Ma.||||Fine to coarse grained, grey to buff, some parts orange in colour.|30-MAR-12
2645|Broome Sandstone|66193|5|Briefly described|p569 Fig.2|Early Cretaceous|Early Cretaceous|in offshore Canning Basin, underlies the Mermaid Formation||||||
2645|Broome Sandstone|67202|5|Briefly described|p43, p44 Fig.2.10, p128|Cretaceous|Cretaceous|One of the dominant aquifers in the Canning Basin. Conductivity image.||||Overlies the Jarlemai Siltstone. Unconformably overlain by the Callawa Formation.||15-FEB-18
2645|Broome Sandstone|68007|5|Briefly described|p4, p8|Early Cretaceous|Early Cretaceous|Canning Basin. Interpreted as about 200m thick in Patience 1 well (near surface to 200m depth), Menzel and Lipski (1986). No biostratigraphic data presented.||||Lateral equivalent of Callawa Formation.|Very light grey, very fine- to very coarse-grained, angular to sub-rounded, quartz sandstone; minor lithic grains, feldspar and mica.|19-FEB-20
2645|Broome Sandstone|68811|5|Briefly described|p77, p78, p79|Cretaceous|Jurassic|Forms extensive platforms and low cliffs. See also p127 tbl 14, p154 app 1, p173 tbl 34. [Age vague. Grouped with Jarlemai Siltstone]||||Unconformably overlies the Jarlemai Siltstone.|Mostly sandstone with minor beds of grey siltstone and claystone.|14-APR-20
2645|Broome Sandstone|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Unconformably overlies Jarlemai Siltstone. Overlain by Samuel and Parda Formations, Frezier and Melligo Sandstones.||18-JAN-17
2645|Broome Sandstone|69029|6|Mentioned|p319|Barremian|Berriasian|Of Canning Basin.||||Overlain by Samuel Formation. Underlain by Bardwire Sandstone.||
2645|Broome Sandstone|69182|6|Mentioned|Ch4 p9, Ch4 p30-p35|Early Cretaceous|Early Cretaceous|Canning Basin. See also Ch4 p45, Ch4 p47, Ch4 p65, Ch4 p83-p84. ||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Frezier Sandstone, Parda Formation and Melligo Sandstone.||10-FEB-20
2645|Broome Sandstone|69297|6|Mentioned|p337, p352|Barremian|Valanginian|Broome Platform of the Canning Basin and Canning Basin. ||||Overlies the Mowla Sandstone. Overlies or is interbedded with the Mermaid Formation. Overlain by the Melligo Sandstone.||
2645|Broome Sandstone|69312|5|Briefly described|p3|Barremian|Berriasian|Canning Basin. ||||Unconformably (or disconformably) overlies the Jarlemai Siltstone. Overlain by the Samuel Formation.|Sandstone.|
2645|Broome Sandstone|69590|4|Described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
2645|Broome Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Cretaceous||||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|
2645|Broome Sandstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Roebuck Basin.||||Overlies Egret Formation. Is overlain by Mermaid Formation.||
2645|Broome Sandstone|70065|5|Briefly described|Rowley: Fig.2; p2. Regional: Fig.4; p4|Barremian|Valanginian|Roebuck Basin and offshore Canning Basin. Delta sands form reservoirs.||||Overlies Baleine Formation. Is overlain and enclosed by Mermaid Formation.||
2645|Broome Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Early Cretaceous|Early Cretaceous||100-145 Ma||||Fine- to coarse-grained sandstone; minor mudstone and conglomerate|10-FEB-20
2645|Broome Sandstone|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Unconformably overlies the Jarlemai Siltstone. Overlain by the Frezier Sandstone, Parda Formation and Melligo Sandstone. Equivalent to the Callawa and Cronin Formations.||10-FEB-20
2645|Broome Sandstone|71267|4|Described|GEOL_LUT_CSV files|Early Cretaceous|Early Cretaceous|Of Canning Basin. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|145-113 Ma (biostrat)||||Fine- to very coarse-grained sandstone; minor mudstone and conglomerate; deltaic|
2645|Broome Sandstone|71601|6|Mentioned|p120 , p121|Barremian|Valanginian|WA. Includes a diverse thyreophoran ichnofauna.||||||
2645|Broome Sandstone|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Unconformably overlies the Jarlemai Formation. Overlain by the Frezier Sandstone, Parda Formation and the Melligo Sandstone.|Sandstone.|10-FEB-20
2645|Broome Sandstone|72034|6|Mentioned|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Shown informally grouped with Mowla and Melligo Sandstones. Siliciclastic Canning Basin unit.  Age from biostratigraphy.||||||
2645|Broome Sandstone|72497|5|Briefly described|p3 Fig.2.|Barremian|Berriasian|Shown as occuring in parts of the Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably underlies Melligo-Para-Frozier Sandstone and is laterally equivalent to Callawa Formation. Unconformably overlies Jarlemai Siltstone, Barbwire and Meda Sandstones.||
2645|Broome Sandstone|72499|4|Described|p7 Fig.6, p10, p70, p89.|Early Cretaceous|Early Cretaceous|Shallow marine to fluvio-deltaic depositional environment. Recorded at the top of the Perindi 1 well log. Considered to host an important shallow groundwater aquifer in the western Canning Basin. Significant thickness (130-250 m) expected in one of the study areas.||||Shown as unconformably overlying Jarlemai Formation, underlies Frezier, Melligo Sandstones, Parda Formation, Samuel Formation. Laterally equivalent to Callawa and Cronin Formations.|Dominantly sandstone.|
2645|Broome Sandstone|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 Frezier Sandstone, Parda Formation, and Melligo Sandstone. Equivalent to Callawa/Cronin formations.|Dominantly sandstone.|
2645|Broome Sandstone|73213|5|Briefly described|955, 957 Fig.2, 958-959, 962, 964|Mesozoic|Mesozoic|See also p 967-968, 971.||||Is overlain unconformably by Mowanjum Sand.|Localy ferruginised or silcreted.|
2656|Brougham sandstone|23350|5|Briefly described|261|||Informal name||||||
2656|Brougham sandstone|40331|4|Described|p12|||||||||
2683|Browne Formation|22589|6|Mentioned|p128,30||Neoproterozoic|||||||
2683|Browne Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
2683|Browne Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
2683|Browne Formation|22907|6|Mentioned|41|||Geol province Officer Basin.||||||24-SEP-08
2683|Browne Formation|23314|5|Briefly described|331|||||||||
2683|Browne Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|~750Ma||||||
2683|Browne Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
2683|Browne Formation|23571|3|Fully described|p1, 7, 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. Underlying Unit: Townsend Quartzite (disconformable) and Lefroy Formation (disconformable?). Overlying Unit: Hussar Formation (conformable). Max. thickness: >2308m. Contains stromatolites.||||||
2683|Browne Formation|24161|4|Described|p9 Fig.6, p11|Neoproterozoic|Neoproterozoic|Disconformably overlies the ?Lefroy Formation. Conformably overlain by the Hussar Formation. Geological Province: Officer Basin.||||||
2683|Browne Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.  See also p12.||||||
2683|Browne Formation|41751|6|Mentioned|p8|||||||||
2683|Browne Formation|43756|6|Mentioned|p541|||||||||
2683|Browne Formation|44111|6|Mentioned|p.58 Fig. 2, p.59|||in Officer Basin. Includes evaporites, stromatolitic carbonates and red beds.||||||
2683|Browne Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
2683|Browne Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Contains halite beds and shales each more than 10m thick. Geological Province: Officer Basin.||||||
2683|Browne Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin. ||Unit in Buldya Group.|||Evaporites, halite.|
2683|Browne Formation|60118|6|Mentioned|p30|||Contains halite beds <10m thick. Geological Province: Officer Basin.||||||
2683|Browne Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. See also p16 Tb. 3.||||||11-APR-08
2683|Browne Formation|61272|5|Briefly described|p120 Fig.1|||Unconformably overlies Lefroy Formation. Overlain by Hussar Formation. See also p123 Fig.4||||||
2683|Browne Formation|61716|5|Briefly described|p642|||Geological Province: Officer Basin.||||||10-MAY-06
2683|Browne Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Willouran|Willouran|Of the Buldya Group. Geological Province: central Officer Basin. See also p81, p131.||||||07-FEB-11
2683|Browne Formation|62453|3|Fully described|p5 Fig. 3, 16, 18|Cryogenian|Cryogenian|Of Buldya Gp. Geol. Prov: Officer Basin. Overlain by Hussar and Kanpa Fm's. Overlies: Townsend Qtzte. Previously Browne Evaporites, Browne Beds, Browne beds. Overlies: Cornelia Sst. Dolomite, lst. Overlies: Lefroy Fm.||||||
2683|Browne Formation|62987|5|Briefly described|p30,p31|||Of the Buldya Group. Geological Province: Officer Basin. Contains major halite intervals.||||||25-JAN-07
2683|Browne Formation|63022|5|Briefly described|p1015, p1016 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Buldya Group. Overlain by Hussar Formation. Geological Province: Officer Basin. Reddish-brown mudstone with halite crystals becoming more abundant towards a basal halite interval.||||||16-JUL-13
2683|Browne Formation|64103|5|Briefly described|p400 Fig. 3|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
2683|Browne Formation|64325|5|Briefly described|p80, p82 Fig. 2|Neoproterozoic|Neoproterozoic|A unit of Supersequence 1. Overlies Lefroy Formation. Geological Province: western Officer Basin. Comprises mudstone, argillaceous siltstone, dolomite and evaporite including halite. Correlative of Alinya Formation in eastern officer Basin in SA. ||||||
2683|Browne Formation|64625|6|Mentioned|p246|||Probably fed by the Gairdner Dyke Swarm.||||||
2683|Browne Formation|64793|5|Briefly described|p283-293|Cryogenian|Cryogenian|Of central Officer Basin. Age inferred from Fig.3.|c.840 - c.818 Ma.|||Overlies Townsend Quartzite unconformably.|Calcareous shale, anhydrite, gypsum, halite, sandstone, dolomite, stromatolitic dolomite, dolomitic limestone and red fine-grained siliciclastic deposits.|
2683|Browne Formation|64796|5|Briefly described|p183 fig 2, p185, p199-201|Cryogenian|Cryogenian|Of Officer Basin.|~830|||Correlated to Bitter Springs Formation and Coominaree Dolomite.|Stromatolitic dolomite, thin-bedded dolomite, shale and massive evaporites.|
2683|Browne Formation|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
2683|Browne Formation|64970|4|Described|p717, p719 Fig. 2, p720|Riphean|Riphean|Overlie Townsend Quartzite. Overlain with apparent conformities by Hurrae, Kanpa and Steptoe Formations. Evaporitic unit consisting of green, red-brown, grey and black shales and silstones. Also on p 721 Fig. 5, 6, 7.||||||
2683|Browne Formation|65102|4|Described|p365,366,367,372 Figs. 4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. Laterally equivalent to Madley and Wright Hill Formations. Conformably overlain by Hussar Formation. 30-4000m; dolomitic limestone, calcareous shale; anhydrite, gypsum & halite; shallow marine and sabkha to playa lake; base of unit not yet intersected in drilling; correlates with Woolnough and Madley Formations; type section in Browne 1, 133-387m.||||||
2683|Browne Formation|65363|3|Fully described|p1, p6 Fig.5, pp10-11, p18.|Neoproterozoic|Neoproterozoic|Officer Basin. Based on presence of Acaciella australica Stromatolite Assemblage, correlates with Skates Hill Formation, and probably lower Mundadjini Formation. The lithologies are decribed in detail. Porosity and permeability are briefly discussed. The remarkable similarity of this unit in widely separated drillholes implies a low topographic gradient across the western platform of the basin during deposition. Thickness increases dramatically (800%) to the northeast.||Unit in Buldya Group.|Includes Woolnough Member, and Lancer Member at the top.|Is overlain  by Hussar Formation. Overlies Cornelia Sandstone with an erosional unconformity or disconformity.|Reddish-brown sandstone and mudstone; halite crystals becoming abundant; red-grey dolostone; grey argillaceous dolostone; fine-grained sandstone; minor conglomerate; un-named halite interval above basal mudstone.|
2683|Browne Formation|65364|5|Briefly described|p81|||Officer Basin.|||Includes Lancer Member, Woolnough Member and an unnamed halite interval.|Overlain by Hussar Formation, may be underlain by Cornelia Sandstone.|Reddish-brown sandstone and mudstone, red-grey dolostone, grey, argillaceous dolostone, halite, minor conglomerate.|16-MAR-12
2683|Browne Formation|65365|4|Described|p1, 3-5, 6, 7, p8 Fig 3, p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group. Western and central Officer Basin.  Includes stromatolite assemblage.|||Includes Lancer and Woolnough Members.|||19-MAR-12
2683|Browne Formation|65366|5|Briefly described|p19, 20, 21, p23 Fig. 3, p24|Cryogenian|Cryogenian|Of the Buldya Group, western Officer Basin. Includes the Woolnough Member. ||||||
2683|Browne Formation|65368|5|Briefly described|p12, 13, 18 p15-16 Fig. 1-2, p17 Fig. 4|Neoproterozoic|Neoproterozoic|Red mudstone, siltstone, and sandstone.||||||19-MAR-12
2683|Browne Formation|65370|6|Mentioned|p39 Tb 1, p41|||In Lancer 1: light brown, medium-grained sandstone. Highest porosity and permeability of samples tested.||||||04-MAY-11
2683|Browne Formation|65371|5|Briefly described|p53, 54 Fig. 1, p55-57|||Of Buldya Group, Officer Basin. Includes Lancer, Woolnough Members. Unconformable on ?Cornelia Sandstone. Conformably overlain by Hussar Formation. Red-brown mudstone, halite, argillaceous dolostone, sandstone, minor conglomerate. Mineralogy discussed.||||||
2683|Browne Formation|65410|6|Mentioned|p72, p76.|Neoproterozoic|Neoproterozoic|Western Officer Basin. Part of Supersequence 1. Contains a palynological assemblage of abundant filaments, mat fragments containing filaments and/or coccoids, clusters of spheres, and abundant leiospheres.||||||
2683|Browne Formation|65416|4|Described|pp137-140, p145.|Middle Neoproterozoic|Middle Neoproterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Lateral equivalent of Bitter Springs Formation (Amadeus Basin). An evaporitic sequence correlated with the Madley Formation (this unit's former name) of the Gibson Sub-basin. Also correlated with Mundadjini and Spearhole Formations.||||Unconformably overlies Townsend Quartzite, Lefroy Formation and Bangemall Group. Is overlain by Hussar Formation conformably, and by Lennis Sandstone, McFadden and Paterson Formations unconformably.|Shale and siltstone, with interbedded halite, anhydrite and dolomite.|
2683|Browne Formation|67195|4|Described|p9 fig5, p10,18, p19 tbl1, p40,45,47,53|Neoproterozoic|Neoproterozoic|Western Officer Basin. Complex internal architecture and dynamic environment of deposition from sabkha through saline-restricted to open marine. Thermal conductivity of 2.64 W/mK. Basal unit of 4 wells in this study. See also App 1.||||Unconformably overlies Lefroy Formation, Townsend Quartzite, overlain by Hussar Formation.|Evaporite/ halite interbedded with dolomite, claystone [shown as cst], shale and mudstone.|
2683|Browne Formation|67200|5|Briefly described|app 2 p9, 10||||||||Halite, dolomite and siltstone.|
2683|Browne Formation|67454|4|Described|pp563-567, p569, p571.|Neoproterozoic|Neoproterozoic|Basal unit of the Officer Basin at the Lancer 1 stratigraphic drillhole. Includes redbeds. Presence of salt implies dry and warm environments, consistent with low-intermediate palaeolatitudes. Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed.|c.830 - 800 Ma (Grey et al. 2005).|Unit in Buldya Group.|Includes Woolnough and Lancer Members.|Unconformably overlies Cornelia Formation. Is overlain by Hussar Formation.|A lower mudstone and evaporite succession, a middle stromatolitic dolostone and mudstone unit (Woolnough Member), and an upper sandstone-dominated unit (Lancer Member).|
2683|Browne Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
2683|Browne Formation|69029|6|Mentioned|p328-330|Neoproterozoic|Neoproterozoic|Of Officer Basin. Contains thin organic-rich source rock shales ranging from fair to good oil potental.||||Overlain by Hussar Formation. Underlain by Lefroy Formation.||
2683|Browne Formation|69091|5|Briefly described|p30 Fig.3.5, p37, see comments|Neoproterozoic|Neoproterozoic|Towards base of Officer Basin.  Rests directly on basement (except Townsend Quartzite is basal unit at northeastern edge of basin). Thickness: several hundred metres, cumulative. Contains numerous evaporite horizons (halite, anhydrite and gypsum).  Misspelled as Bowne Formation on p45. See also p38 Fig.3.7, p41 Fig.3.8, p43, p44-45, p81 Fig.4.17, p108 Fig.5.9, p174 Fig.9.5, p177 Fig.9.6, p182, p200 Fig.10.2||Buldya Group||Is unconformably overlain by Table Hill Volcanics.|Sedimentary.|26-SEP-14
2683|Browne Formation|69438|6|Mentioned|p23:11|||Western Officer Basin.||||Is correlated with the Bitter Springs Formation (Amadeus Basin).||12-JUL-16
2683|Browne Formation|70793|5|Briefly described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.||Unit of Buldya Group.||||
2683|Browne Formation|71001|6|Mentioned|p22|||Officer Basin.||||Is overlain by Hussar Formation.|Stromatolitic dolostone.|
2683|Browne Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||crystalline dolostone/dolomite, anhydrite, rock salt, gypsum|
2683|Browne Formation|71268|5|Briefly described|100k_interpgeop_lut.csv|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.||Unit of Buldya Group.||Underlain by Townsend Quartzite.||
2683|Browne Formation|71288|6|Mentioned|p136|Neoproterozoic|Neoproterozoic|An 830-730 Ma paleopole position from this unit locates Australia in low latitudes.|830-730 Ma.|||||
2683|Browne Formation|73086|6|Mentioned|p15, p30, p57, p148|||Officer Basin. Correlation with Bitter Springs groups is based on isotopic and other geochemical studies.||||May correlate to Bitter Springs Group and Wallara Formation [and Coominaree Dolomite?].||
2724|Brunos Band|43290|6|Mentioned|p6||Archean|of Mount Sylvia Formation.  Informal name.||||||07-NOV-08
2724|Brunos Band|67201|5|Briefly described|p52, p55|||Informal name. The uppermost BIF in Mount Sylvia Formation, Brunos Band, is a prominent stratigraphic marker bed across the whole Basin.||Mount Sylvia Formation||||22-NOV-16
2793|Buckland Point Member|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
2793|Buckland Point Member|32728|5|Briefly described|p38|||||||||
2793|Buckland Point Member|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
2793|Buckland Point Member|36885|4|Described|p185|||||||||
2793|Buckland Point Member|64748|5|Briefly described|p269 Tb.1|Statherian||Locally at the top of the Warton Sandstone; quartzose and ferruginous sandstone; ||||||
2793|Buckland Point Member|69634|4|Described|250k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1835-1740 Ma (Inferred)|Unit of Warton Sandstone.|||Quartz sandstone, white, thick-bedded, medium, blocky to flaggy; interbedded with ferruginous sandstone, red to red-brown thin-bedded, fine, flaggy; and ferruginous siltstone|
2793|Buckland Point Member|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Warton Sandstone.||Is overlain by Elgee Siltstone.|Thick-bedded, blocky to flaggy quartz sandstone interbedded with ferruginous sandstone and siltstone.|
2793|Buckland Point Member|70154|5|Briefly described|250k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 250k_interpgeop_lut.csv.|1740-1835 Ma||||Thick-bedded, blocky to flaggy quartz sandstone interbedded with ferruginous sandstone and siltstone|
2793|Buckland Point Member|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Warton Sandstone.||Is overlain by Elgee Siltstone.|Thick-bedded, blocky to flaggy quartz sandstone interbedded with ferruginous sandstone and siltstone.|
2793|Buckland Point Member|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: King Leopold Orogen. Of Kimberley Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 1m_interpgeop_lut.csv.|1834-1740 Ma (inferred)|Unit of Warton Sandstone.|||Thick-bedded, blocky to flaggy quartz sandstone interbedded with ferruginous sandstone and siltstone|
2808|Buddadoo Gabbro|30973|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
2808|Buddadoo Gabbro|32337|4|Described|p10|||||||||
2808|Buddadoo Gabbro|35726|6|Mentioned|p94|||||||||
2808|Buddadoo Gabbro|36551|6|Mentioned|p141|||||||||
2808|Buddadoo Gabbro|41594|4|Described|p65|||||||||
2808|Buddadoo Gabbro|70769|5|Briefly described|Map legend.|Archean|Archean|Murchision Domain, Youanmi Terrane, Yilgarn Craton.|c.2813 Ma.|Meeline Suite.|||Layered gabbroic rocks with distinctive magnetitite horizons and minor diorite. Separately-mapped: magnetitite layers up to 1m thick comprising 15mm magnetite crystals interlayered with leucogabbro with 5-10mm grainsize. Both metamorphosed.|
2808|Buddadoo 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, 500k_interpgeop_lut.csv, Badja100_2240_stratig.pdf. Numerous additional lithologies are discussed.|ca 2813 Ma (inferred)|Meeline Suite|||Gabbro with magnetitite layers up to 1 m thick comprising 15 mm magnetite crystals interlayered with leucogabbro with 510 mm grain size; metamorphosed. Minor diorite|
2808|Buddadoo Gabbro|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
2808|Buddadoo 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.|2813 Ma (inferred)|Unit of Meeline Suite.|||Layered gabbroic rocks with distinctive magnetitite horizons and minor diorite; metamorphosed|
2833|Bugle Gap Limestone|22741|5|Briefly described|P21, P24, Table3 P16||Devonian|||||||
2833|Bugle Gap Limestone|31152|6|Mentioned|Fig. 3|||||||||
2833|Bugle Gap Limestone|31332|6|Mentioned|Fig. 3|||||||||
2833|Bugle Gap Limestone|32594|6|Mentioned|p3|||Refers Playford & Lowry (1966)||||||
2833|Bugle Gap Limestone|32647|6|Mentioned|Fig. 24|||||||||
2833|Bugle Gap Limestone|32865|6|Mentioned|p472|||See also p474. Fauna||||||28-JAN-20
2833|Bugle Gap Limestone|32979|6|Mentioned|p38|||Correlation with basins in India||||||
2833|Bugle Gap Limestone|33042|6|Mentioned|p725|||See also pp727,733,745,749 etc. Famennian||||||28-JAN-20
2833|Bugle Gap Limestone|34427|6|Mentioned|Fig.3|||||||||
2833|Bugle Gap Limestone|35104|6|Mentioned|p5|||||||||
2833|Bugle Gap Limestone|36225|6|Mentioned|Map legend|Famennian|Famennian|||||||
2833|Bugle Gap Limestone|36890|3|Fully described|p333|||||||||
2833|Bugle Gap Limestone|38207|6|Mentioned|Fig.1|||||||||
2833|Bugle Gap Limestone|38263|6|Mentioned|p16|||||||||
2833|Bugle Gap Limestone|40793|6|Mentioned|Fig.3|||||||||
2833|Bugle Gap Limestone|40797|6|Mentioned|Fig.2|||||||||
2833|Bugle Gap Limestone|41139|6|Mentioned|Fig.2|||||||||
2833|Bugle Gap Limestone|42030|5|Briefly described|p748|||||||||
2833|Bugle Gap Limestone|42111|6|Mentioned|Text fig.3 P90|||||||||
2833|Bugle Gap Limestone|42351|5|Briefly described|Fig.3 P40|||||||||
2833|Bugle Gap Limestone|42564|5|Briefly described|Fig.5, 6 P6|||||||||
2833|Bugle Gap Limestone|42994|5|Briefly described|p212|||||||||
2833|Bugle Gap Limestone|43563|6|Mentioned|Fig.5,p10||Late Devonian|||||||
2833|Bugle Gap Limestone|43723|6|Mentioned|p51||Devonian|||||||
2833|Bugle Gap Limestone|44143|4|Described|p.438 Table 4-19; p442, p443 Figure 4-98|Famennian|Famennian|Up to 180m thick; calcarenite, calcirudite, and magabreccia; shallow marine. Interfingers with Windjana Limestone. Type section 5km SE of Lloyd Hill (MOUNT RAMSAY: 18deg 42' S, 126deg 04' E). Contains sparse fauna of brachiopods and conodonts.||||||22-NOV-17
2833|Bugle Gap Limestone|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Fore-reef subfacies; calcarenite, limestone breccia and megabreccia.  Geological Province: Canning Basin.||||||18-MAY-05
2833|Bugle Gap Limestone|44397|14|Not recorded|p.12,Fig.3,Table 4||Famennian|E52-9.||||||
2833|Bugle Gap Limestone|44398|14|Not recorded|map legend||Famennian|||||||
2833|Bugle Gap Limestone|44998|2|Defined|p.37||Devonian|On many pages. p.26,38-9,42-3,50.||||||
2833|Bugle Gap Limestone|45015|5|Briefly described|p59|Devonian|Devonian|Probably same age as Willaraddie Formation. Geological Province: Fitzroy Basin.||||||01-JUN-06
2833|Bugle Gap Limestone|45039|4|Described|p21|||Upper Devonian||||||
2833|Bugle Gap Limestone|45041|6|Mentioned|Fig.45|||Famennian||||||
2833|Bugle Gap Limestone|45101|4|Described|p7|||See also P22, conodont content||||||
2833|Bugle Gap Limestone|45133|6|Mentioned|p4|||||||||
2833|Bugle Gap Limestone|45143|6|Mentioned|Fig.3|||Time-stratigraphic interpretations.||||||
2833|Bugle Gap Limestone|45153|2|Defined|App.3-37|late Famennian|late Famennian|||||||
2833|Bugle Gap Limestone|45158|4|Described|p24|||||||||
2833|Bugle Gap Limestone|48826|14|Not recorded|p.19,20|||Tb.III||||||
2833|Bugle Gap Limestone|48831|14|Not recorded|p.45,49,64|||||||||
2833|Bugle Gap Limestone|48848|14|Not recorded|p.40,46|||||||||
2833|Bugle Gap Limestone|63938|5|Briefly described|p49 Fig.1, p50 Fig.2|Famennian|Famennian|||||||
2833|Bugle Gap Limestone|64502|6|Mentioned|p766 Fig.3||Devonian|||||||
2833|Bugle Gap Limestone|64580|5|Briefly described|map legend|||Famennian reef complexes, marginal slope and basin facies.||||||10-NOV-08
2833|Bugle Gap Limestone|64643|5|Briefly described|p5 Fig. 4, p18, 34, 35|Famennian|Famennian|Marginal slope facies, fore-reef facies.||||||10-NOV-08
2833|Bugle Gap Limestone|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
2833|Bugle Gap Limestone|65486|6|Mentioned|p18, p50 Fig. 67, Plate 1.|Famennian|Famennian|Marginal-slope and basin limestone, sandstone, and siltstone, Canning Basin. A glacial pavement indicated Early Permian ice sheet movement to N or NNW.||||||
2833|Bugle Gap Limestone|66127|3|Fully described|pp57-61, p213, Plates 4, 5, 7, 8.|Famennian|Famennian|Of Guppy et al. (1958). Type section is near the SW end of Bugle Gap. Poorly-preserved glacial pavement showed northerly ice movement in the Permian. Relatively sparse fossils.||||Overlies and interfingers with Virgin Hills Formation. Unconformably underlies Fairfield Group and Carolyn Formation (Grant Group).|Fore-reef subfacies: crudely bedded, pale grey limestone with some allochthonous blocks of reef limestone; sandstone and siltstone.|
2833|Bugle Gap Limestone|67131|6|Mentioned|p3 Fig. 2|Famennian|Famennian|Marginal slope facies.||||Overlies Virgin Hills Formation; overlain by Gumhole Formation.||28-JAN-20
2833|Bugle Gap Limestone|69099|5|Briefly described|500k_geologyp08_lut.csv|Fammenian|Fammenian|Famennian reef complexes, marginal slope and basin facies. Grouped as Piker Hills Formation, Bugle Gap Limestone, upper Napier Formation and upper Virgin Hills Formation in 500k_geologyp08_lut.csv.||||||
2833|Bugle Gap Limestone|69165|6|Mentioned|500k_geologyp08_lut.csv|Famennian|Famennian|||||||
2833|Bugle Gap Limestone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fossiliferous, shallow marine reef complex marginal slope facies, white to pink medium to thickly bedded calcarenite grading to calcirudite|
2848|Buldania Formation|23136|6|Mentioned|p265 Fig.1|||||||||
2848|Buldania Formation|30562|2|Defined|p13|Archean|Archean|See also p7. Basic volcanic rocks intruded by basic and ultrabasic rocks. Possibly equivalent to Woolyeenyer Formation.||||||17-FEB-14
2848|Buldania Formation|30959|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
2848|Buldania Formation|36869|6|Mentioned|p48|||||||||
2848|Buldania Formation|41432|5|Briefly described|p13|||||||||
2848|Buldania Formation|60076|6|Mentioned|p16 Fig. 6|||Probably of the Buldania Granitoid Complex?||||||01-FEB-05
2848|Buldania Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|SE Kambalda Domain. Kambalda Sequence.|||||Tholeiitic and high MgO basalt.|
2884|Bullabulling Monzogranite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Foliated, partly recrystallized monzogranite with scattered microcline phenocrysts|
2884|Bullabulling Monzogranite|41914|4|Described|p20|||Reserved as Bullabulling Member||||||
2884|Bullabulling Monzogranite|68066|5|Briefly described|p5 Fig. 2, p26, map|Archean|Archean|Outcrops between a foliated margin of Burra Monzogranite and the western limit of the Coolgardie greenstone belt. Appears to be a finer grained enclave of Burra Monzogranite.|||||Foliated, partly recrystallized monzogranite; quartz-biotite-oligoclase-microcline matrix and scattered microcline phenocrysts.|
2884|Bullabulling Monzogranite|69152|4|Described|1m_geologyp08_lut.csv|Archean|Archean||||||Foliated, partly recrystallised monzogranite with scattered microcline phenocrysts; low-Ca granite.|05-AUG-15
2884|Bullabulling Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
2884|Bullabulling Monzogranite|71270|5|Briefly described|1m_geologyp12_lut.csv|||Geological province: Yilgarn Craton, West Australian Craton. |||||Foliated, partly recrystallised monzogranite with scattered microcline phenocrysts; low-Ca granite|
2887|Bullara Limestone|24351|5|Briefly described|Plate 4 (in pocket)|Early Miocene|Late Oligocene|Geological Province: Exmouth Sub-basin (onshore).||||||13-DEC-07
2887|Bullara Limestone|37016|6|Mentioned|Map legend|Miocene|Miocene|||||||
2887|Bullara Limestone|39427|4|Described|Table 1|||||||||
2887|Bullara Limestone|40617|6|Mentioned|p18|||||||||
2887|Bullara Limestone|41271|3|Fully described|p178|||Of Cape Range Group.||||||
2887|Bullara Limestone|46805|2|Defined|p171|late Oligocene|late Oligocene|||||||
2887|Bullara Limestone|46983|6|Mentioned|Fig.2|||||||||
2887|Bullara Limestone|61155|5|Briefly described|p15|Early Miocene|Late Oligocene|Of the Cape Range Group. Age: 24.5-~21Ma. Max. thickness: 100m.  Geological Province: Carnarvon Basin /onshore.||||||03-MAR-10
2887|Bullara Limestone|62837|5|Briefly described|Stratigraphic columns|Oligocene|Oligocene|Age: >25-20Ma. Geological Province: Exmouth Sub-basin.||||||01-MAR-10
2887|Bullara Limestone|70066|5|Briefly described|Regional: Fig.6|Aquitanian|Chattian|Exmouth Sub-basin, Northern Carnarvon Basin.||||Overlies Mandu Limestone. Is overlain by Tulki Limestone.||
2914|Bullita Group|9538|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Siltstone, minor dolomite.   Age: ~900Ma.||||||
2914|Bullita Group|14019|5|Briefly described|p2 Fig. 1|||Geological Province: Victoria Basin.||||||
2914|Bullita Group|23216|6|Mentioned|Fig3p5||Mesoproterozoic|||||||
2914|Bullita Group|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Victoria Basin.  Correlates with Lower Wade Creek Formation (Victoria Basin) and Nathan Group (Ashburton Province).||||||17-MAR-05
2914|Bullita Group|24122|3|Fully described|p3, p5 Tb.1|Proterozoic|Proterozoic|Includes the Bynoe, Skull Creek and Timber Creek Formations. Unconformably overlain by Tijunna Group, overlies Wattie Group.  Geological Province: Victoria Basin.||||||25-JAN-10
2914|Bullita Group|24297|3|Fully described|p8|Proterozoic|Proterozoic|Consists of Battle Creek Formation, Weaner Sandstone, Bynoe Formation, Skull Creek Formation and Timber Creek Formation.  See also p5 Tb. 2.||||||28-SEP-11
2914|Bullita Group|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
2914|Bullita Group|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin|||Includes Timber Creek Formation, Skull Creek Formation, Bynoe Formation.|||14-MAR-18
2914|Bullita Group|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Overlies the Wattie Group. Unconformably overlain by Tijunna Group. Geological Province: Victoria Basin.||||||25-JAN-06
2914|Bullita Group|24442|5|Briefly described|p50 Fig. 1|||Divided into 8 units.  Geological Province: Victoria Basin.||||||
2914|Bullita Group|28255|3|Fully described|p43, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Subdivided into seven formations/units.||||||07-JUN-05
2914|Bullita Group|30003|4|Described|p7, p13|||Age is Carpentarian or Adelaidean.||||||19-APR-05
2914|Bullita Group|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
2914|Bullita Group|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
2914|Bullita Group|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||02-DEC-04
2914|Bullita Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2914|Bullita Group|32660|4|Described|Table 6|||||||||
2914|Bullita Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Timber Creek and Skull Creek Formations.||||||02-DEC-04
2914|Bullita Group|32700|3|Fully described|Table 1|||See also p13||||||02-AUG-06
2914|Bullita Group|32701|4|Described|Table 1|||Adelaidean. See also p8||||||02-AUG-06
2914|Bullita Group|32728|6|Mentioned|p16|||||||||
2914|Bullita Group|32775|5|Briefly described|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||02-DEC-04
2914|Bullita Group|33373|3|Fully described|p9|||Table 2.||||||
2914|Bullita Group|33374|6|Mentioned|p6|||Stratigraphy.||||||
2914|Bullita Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2914|Bullita Group|33377|5|Briefly described|Table 2|||||||||
2914|Bullita Group|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||27-APR-05
2914|Bullita Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
2914|Bullita Group|37462|4|Described|Table 4.IV|||||||||
2914|Bullita Group|37579|5|Briefly described|Regional setting map legend|Adelaidean|Adelaidean|Siltstone, minor dolomite.  Probably Adelaidean||||||10-OCT-05
2914|Bullita Group|38157|6|Mentioned|p284|||||||||
2914|Bullita Group|38243|6|Mentioned|p355|||||||||
2914|Bullita Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
2914|Bullita Group|39563|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
2914|Bullita Group|39801|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Prob.Late Proterozoic. Siltstone; minor dolomite.||||||04-OCT-05
2914|Bullita Group|40105|6|Mentioned|Fig.3|||||||||
2914|Bullita Group|40168|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Siltstone, minor dolomite.||||||18-OCT-05
2914|Bullita Group|40223|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, minor dolomite.||||||19-OCT-05
2914|Bullita Group|40823|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
2914|Bullita Group|41407|6|Mentioned|Map legend|Mesoproterozoic||||||||
2914|Bullita Group|41586|6|Mentioned|Map legend|||||||||
2914|Bullita Group|41645|6|Mentioned|Fig.4|||||||||
2914|Bullita Group|41646|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Siltstone, dolomite, sandstone.||||||17-OCT-05
2914|Bullita Group|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Siltstone, dolomite, sandstone.||||||07-OCT-05
2914|Bullita Group|41661|6|Mentioned|Fig.5|||||||||
2914|Bullita Group|42012|6|Mentioned|p13|||||||||
2914|Bullita Group|45112|3|Fully described|p19|||||||||
2914|Bullita Group|45140|6|Mentioned|p13|||Victoria River region.||||||
2914|Bullita Group|46675|5|Briefly described|Map legend for regional setting...|Mesoproterozoic|Mesoproterozoic|Siltstone; minor dolomite.  Geological Province: Pine Creek Geosyncline.||||||
2914|Bullita Group|46864|6|Mentioned|Fig.4|||||||||
2914|Bullita Group|48938|2|Defined|p22|Proterozoic|Proterozoic|See also p24. ?Adelaidean.||||||02-AUG-06
2914|Bullita Group|48942|3|Fully described|p44|||See also pp45-57.||||||02-AUG-06
2914|Bullita Group|48943|2|Defined|p50|Proterozoic|Proterozoic|?Adelaidean.||||||
2914|Bullita Group|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Includes: Timber Creek Formation, Skull Creek Formation. Dolostone, dolarenite, siltstone, sandstone||||||23-JUL-04
2914|Bullita Group|60526|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Siltstone; minor dolomite.||||||
2914|Bullita Group|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone and dolostone. Overlies Wattie Group unconformably. Overlain unconformably by Tijunna Group. Geological Province: Victoria Basin.||||||
2914|Bullita Group|60682|4|Described|piii|Mesoproterozoic|Mesoproterozoic|Conformably overlies: Wattie Group. Age: 1610-1570Ma. Contains 6 formations. Geological Province: Victoria Basin.||||||
2914|Bullita Group|60685|5|Briefly described|p4 Fig. 3, p8|Mesoproterozoic|Paleoproterozoic|Dolostone, siltstone, sandstone - high carbonate content. Conformable on the Wattie Group. Age: 1.61-1.57Ga. Geological Province: Victoria Basin.||||||07-NOV-08
2914|Bullita Group|61573|5|Briefly described|p676, p678 Fig. 3|Mesoproterozoic|Mesoproterozoic|Includes Skull Creek and Bynoe Formations. Siltstone, sandstone, dolostone, chert. Overlain by the Tijunna Group. Probably correlates with the Nathan Group (McArthur Basin). Geological Province: Victoria Basin.||||||
2914|Bullita Group|64724|5|Briefly described|p45 Fig.5, p46|Calymmian|Statherian|Victoria River and Birrindudu Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
2914|Bullita Group|65331|5|Briefly described|Map legend + overview geology map legend|Mesoproterozic|Mesoproterozic|Of Victoria Basin. Includes Skull Creek Formation, Timber Creek Formation. Dolostone, dolarenite, siltstone, sandstone||||||
2914|Bullita Group|65342|5|Briefly described|pp10-11.|||Victoria Basin.|||Includes Timber Creek, Skull Creek, Bynoe, Banyan and Battle Creek Formations; Nero Siltstone; Mount Gordon and Weaner Sandstones.|Overlies Wattie Group. Is unconformably overlain by Tijunna Group.|Several carbonate units and sandstones; minor thin black shale units.|
2914|Bullita Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Timber Creek, Skull Creek and Bynoe Formations.|Unconformably overlies Wattie Group. Is unconformably overlain by Tijunna Group.||
2914|Bullita Group|68733|5|Briefly described|p177, p179 Tb.1, p181-185|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013).|||Includes Timber Creek Formation, Battle Creek Formation, Weaner Sandstone, Bynoe Formation, Skull Creek Formation.|||05-DEC-17
2914|Bullita Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|Southern Birrindudu Basin.|||||Includes stromatolitic carbonate rocks and sandstone deposited in sag basins.|12-JUL-16
2914|Bullita Group|69432|4|Described|p17:1-3. 9-14|||Birrindudu Basin. Had been included in the Victoria Basin by Cutovinos et al. (2002), but is now assigned to the Birrindudu Basin. Is gently folded into broad domes, anticlines and synclines 10-50km across. Exploration target for base metals (brief description).|||Timber Creek, Skull Creek, Bynoe, Banyan, Battle Creek Formations; Nero Siltstone; Mount Gordon, Weaner Sandstones.|Unconformably overlies Wattie Group. Is overlain unconformably by Tijunna Group.|The lower part is mainly stromatolitic carbonates and subordinate siliciclastic rocks deposited on a shoaling, shallow-marine platform. Above that is a transition to siliciclastic deposits.|12-JUL-16
2914|Bullita Group|69441|5|Briefly described|p26:3 Tb. 26.1||||||Timber Creek, Skull Creek Formations.|Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group).||12-JUL-16
2914|Bullita Group|69445|5|Briefly described|p30:4|Proterozoic|Proterozoic|Victoria River region, Birrindudu Basin.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
2914|Bullita Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35|Paleoproterozoic|Paleoproterozoic||||Includes Timber Creek Formation, Skull Creek Formation, Nero Siltstone, Bynoe Formation, Banyan Formation, Mount Gordon Sandstone, Weaner Sandstone, Battle Creek Formation,|Unconformably overlies Wattie Group, unconformably overlain by Tijunna Group||
2914|Bullita Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].|||Includes Skull Creek Formation, Timber Creek Formation.|||18-JUL-16
2914|Bullita Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Bynoe Formation, Skull Creek Formation, Timber Creek Formation.|Unconformably overlies Wattie Group. Is unconformably overlain by Tijunna Group, Auvergne Group.||
2914|Bullita Group|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Timber Creek, Skull Creek, Bynoe Formations.|Is overlain unconformably by Tijunna Group.||
2914|Bullita Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Timber Creek, Skull Creek Formations; Nero Siltstone; Mount Gordon Sandstone.|Unconformably overlies Wattie Group. Is overlain unconformably by Tijunna Group.|Dolostone, sandstone, siltstone, shale.|
2914|Bullita Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Timber Creek, Skull Creek, Bynoe, Battle Creek Formations; Weaner Sandstone.|Overlies Wattie Group. Is overlain unconformably by Tijunna Group.|Dolostone, sandstone, chert, siltstone, shale.|
2914|Bullita Group|70968|5|Briefly described|p6, p115, p120, p124, p130, p132, p138|||Birrindudu Basin.|||Bynoe Formation.|Is overlain unconformably by Roper or Tijunna Groups, or Jasper Gorge Sandstone (Auvergne Group). Equivalent to the Nathan Group.||
2914|Bullita Group|71059|5|Briefly described|p7|||Birrindudu Basin.||||Is overlain unconformably by Roper Group. Equivalent to Nathan Group (McArthur Basin).||
2914|Bullita Group|71169|5|Briefly described|p71|Calymmian|Calymmian|North Australian Craton.|c. 1550-1400 Ma|||||
2914|Bullita Group|71302|5|Briefly described|p1,3,6,22,28,72-74||Paleoproterozoic|Of Birindudu Basin.|||Includes Banyan Formation, Battle Creek Formation, Mount Gordon Sandstone, Weaner Sandstone, Nero Siltstone, Bynoe Formation, Skull Creek Formation, Timber Creek Formation.|Overlain by Tijunna Group. Underlain by Wattie Group.||
2914|Bullita Group|71374|6|Mentioned|p2|||Birrindudu Basin.||||||
2914|Bullita Group|72373|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin. Broadly equivalent to Favenc package, Nathan, Mount Rigg, Balma groups and Karns Dolostone (McArthur Basin) and Namerinni Group (Tomkinson province).||||||
2914|Bullita Group|72718|6|Mentioned|p7|||Birrindudu Basin.|||Banyan Formation, Battle Creek Formation, Weaner Sandstone, Nero Siltstone, Bynoe Formation, Skull Creek Formation, Timber Creek Formation|Underlain by Seale Sandstone (Wattie Group). Overlain[?] by Wondoan Hill Formation (Tijunna Group).||
2934|Bulong Complex|30956|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
2934|Bulong Complex|32268|4|Described|p21|||||||||
2934|Bulong Complex|32269|6|Mentioned|p313|||||||||
2934|Bulong Complex|32271|5|Briefly described|p473|||||||||
2934|Bulong Complex|32694|6|Mentioned|Fig.1|||||||||
2934|Bulong Complex|33837|6|Mentioned|Fig.2|||||||||
2934|Bulong Complex|33847|2|Defined|p18|Archean|Archean|See also p19.||||||07-NOV-08
2934|Bulong Complex|34715|6|Mentioned|p133|||||||||
2934|Bulong Complex|35024|5|Briefly described|p221|||||||||
2934|Bulong Complex|35468|6|Mentioned|p20|||||||||
2934|Bulong Complex|35469|6|Mentioned|p44|||Also shown on Fig.9||||||
2934|Bulong Complex|35726|6|Mentioned|p115|||||||||
2934|Bulong Complex|36869|6|Mentioned|p40|||||||||
2934|Bulong Complex|38474|4|Described|p1776|||||||||
2934|Bulong Complex|38995|6|Mentioned|p4|||||||||
2934|Bulong Complex|41594|4|Described|p67|||||||||
2934|Bulong Complex|43075|6|Mentioned|p10|||||||||
2934|Bulong Complex|43496|6|Mentioned|8|||||||||
2934|Bulong Complex|60076|5|Briefly described|p12 Tb. 2, p18|||Layered cumulates, komatiites; ponded flows up to 400m thick.  Max. thickness of unit: ~5000m.  Geological Province: Gindalbie domain (Yilgarn Craton).||||||01-FEB-05
2934|Bulong Complex|64715|6|Mentioned|p1|Archaean|Archaean|||||||
2934|Bulong Complex|64775|6|Mentioned|p12-1|Neoarchean|Neoarchean||2705 +/- 4 Ma.||||Ultramafics, interleaved with mafic and metamorphosed felsic volcanics.|30-MAR-12
2934|Bulong Complex|65264|6|Mentioned|p16|||Represents a substantial accumulation of ultramafic lava in the Gindalbie area.||||||07-FEB-11
2934|Bulong Complex|66880|5|Briefly described|p9, p27. |Archean|Archean|Gindalbie Terrane. Feldspathic sandstones are same age and composition as in the Kurnalpi Sequence. Possibly an exotic block caught up in the suture between Kalgoorlie and Gindalbie Terranes.|2708 +/- 5 Ma.||||Komatiitic and high MgO dolerite rocks structurally interleaved with calc-alkaline feldspathic sandstones.|
2934|Bulong Complex|70153|5|Briefly described|100726.1.pdf||||2705 +/- 4 Ma (U-Pb SHRIMP zircon: Nelson 1997).||||Includes mafic lavas interbedded with felsic volcaniclastics including tuffaceous zones and cognate clasts.|
2935|Bulyairdie Monzogranite|42741|5|Briefly described|map legend|Archean||||||||07-NOV-08
2935|Bulyairdie Monzogranite|43075|5|Briefly described|p9|||||||||
2935|Bulyairdie Monzogranite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
2935|Bulyairdie Monzogranite|60076|5|Briefly described|p23, p45 App. 1|Archean|Archean|[Agmby]   Medium-grained, hornblende bearing, perthitic K-feldspar phenocrysts; unfoliated.||||||07-NOV-08
2935|Bulyairdie Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium-grained, hornblende monzogranite; perthitic K-feldspar megacrysts.||||||07-FEB-11
2935|Bulyairdie Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained hornblende monzogranite; perthitic K-feldspar megacrysts.|05-AUG-15
2935|Bulyairdie Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained hornblende monzogranite; perthitic K-feldspar megacrysts.|
2935|Bulyairdie Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
2935|Bulyairdie Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. See 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|||||Medium-grained hornblende monzogranite; perthitic K-feldspar megacrysts|
2950|Bunbury Basalt|12525|6|Mentioned|p34.|||One of several Large Igneous Provinces within or close to the west Australian margin up till c.110 Ma, following breakup of Gondwana.||||||
2950|Bunbury Basalt|12758|5|Briefly described|p21, p26|Neocomian|Neocomian|Porphyritic basalt extruded extensively as lava flows over Eastern Bunbury Trough - probably during late stages of Parmelia Group, as implied by palynological evidence. Geological Province: Bunbury Trough (Perth Basin).  See also p57.||||||
2950|Bunbury Basalt|14227|5|Briefly described|p6, Enlcos. 2|Valanginian|Berriasian|||||||07-FEB-11
2950|Bunbury Basalt|22820|4|Described|p23|Cretaceous|Early Cretaceous|Of Warnbro Group. Age: at least 90Ma. Thickness: up to 174m. Geological province: widespread in the onshore part of southern Perth Basin. Consists of lava flows within valleys eroded into the Yarragadee Formation. Sills are porphyritic or microprophyritic||||||19-FEB-13
2950|Bunbury Basalt|23788|5|Briefly described|p9|Early Cretaceous|Early Cretaceous|See also p37. Geological Province: Yilgarn Craton.||||||21-JUL-09
2950|Bunbury Basalt|23816|4|Described|p251, 252|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Overlying unit: Coastal Limestone (surface exposures) and Leederville Formation (subsurface). Max. thickness: 85 m.||||||27-APR-05
2950|Bunbury Basalt|24160|5|Briefly described|p94|Cretaceous|Cretaceous|Perth Basin.|||||Vesicular porphyritic basalt.|
2950|Bunbury Basalt|24443|5|Briefly described|Fig.31|Early Cretaceous|Early Cretaceous|Overlies Parmelia Group. Unconformably overlain by Warnbro Group. Geological Province: Perth Basin.||||||
2950|Bunbury Basalt|29693|6|Mentioned|p34|||||||||
2950|Bunbury Basalt|30188|2|Defined|p76|Early Cretaceous|Early Cretaceous|Refs to Edwards(1938), Trendall(1963).||||||11-APR-08
2950|Bunbury Basalt|30266|6|Mentioned|p93|||||||||
2950|Bunbury Basalt|30308|6|Mentioned|Fig.1|||||||||
2950|Bunbury Basalt|31051|6|Mentioned|p75|||||||||
2950|Bunbury Basalt|31562|6|Mentioned|p11|||||||||
2950|Bunbury Basalt|32104|6|Mentioned|p6|||Refers dates||||||
2950|Bunbury Basalt|33622|6|Mentioned|p92|||Early Cret.||||||21-JUL-09
2950|Bunbury Basalt|33626|6|Mentioned|p715|||||||||
2950|Bunbury Basalt|33627|6|Mentioned|p595|||||||||
2950|Bunbury Basalt|35617|6|Mentioned|p370|||Location of chert.||||||
2950|Bunbury Basalt|36293|2|Defined|p195|Neocomian|Neocomian|Prob. Neocomian.||||||11-APR-08
2950|Bunbury Basalt|36890|3|Fully described|p251|||Formerly Bunbury Lava flow.||||||11-APR-08
2950|Bunbury Basalt|37309|5|Briefly described|p16|||||||||
2950|Bunbury Basalt|37341|6|Mentioned|p230|||||||||
2950|Bunbury Basalt|37350|6|Mentioned|p376|||||||||
2950|Bunbury Basalt|37354|6|Mentioned|p558|||||||||
2950|Bunbury Basalt|37360|6|Mentioned|p581|||||||||
2950|Bunbury Basalt|37364|6|Mentioned|p1051|||||||||
2950|Bunbury Basalt|37499|6|Mentioned|Fig.1|||||||||
2950|Bunbury Basalt|37818|6|Mentioned|p82|||||||||
2950|Bunbury Basalt|38231|4|Described|p465|||||||||
2950|Bunbury Basalt|38479|4|Described|p16|||||||||
2950|Bunbury Basalt|38777|4|Described|p29|||||||||
2950|Bunbury Basalt|39211|6|Mentioned|p61|||||||||
2950|Bunbury Basalt|39794|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2950|Bunbury Basalt|39915|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2950|Bunbury Basalt|40304|3|Fully described|p38|||||||||
2950|Bunbury Basalt|40305|4|Described|p76|||||||||
2950|Bunbury Basalt|40358|4|Described|p22|||||||||
2950|Bunbury Basalt|40359|4|Described|p22|||||||||
2950|Bunbury Basalt|40360|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
2950|Bunbury Basalt|40367|6|Mentioned|p81|||||||||
2950|Bunbury Basalt|41171|6|Mentioned|p170|||||||||
2950|Bunbury Basalt|41341|6|Mentioned|p27|||||||||
2950|Bunbury Basalt|41782|5|Briefly described|p23|||||||||
2950|Bunbury Basalt|42194|5|Briefly described|p5|||See also p38.||||||23-SEP-18
2950|Bunbury Basalt|42434|4|Described|p5|||||||||
2950|Bunbury Basalt|42687|6|Mentioned|map legend|||||||||
2950|Bunbury Basalt|42688|6|Mentioned|map legend|||||||||
2950|Bunbury Basalt|43096|5|Briefly described|p5|||see also Fig.2.||||||
2950|Bunbury Basalt|43189|5|Briefly described|Map Legend|Cretaceous|Jurassic|||||||
2950|Bunbury Basalt|43212|6|Mentioned|p6||Neocomian|||||||
2950|Bunbury Basalt|43308|5|Briefly described|Map Legend||Cretaceous|||||||
2950|Bunbury Basalt|43592|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|||||||
2950|Bunbury Basalt|43789|5|Briefly described|p147|||||||||
2950|Bunbury Basalt|44144|4|Described|p504 Tb.4-21, p516-517, p524|Early Cretaceous|Early Cretaceous|Type Section: Bunbury Beach 33o19'30''S 115o37'40''E. 85m thick subaerial volcanic flows. A dolerite in Sue 1 dated at 136 +/- 3 Ma may be comagmatic.||||Overlies Yarragadee Formation unconformably. Is overlain by Warnbro Group.|Vesicular, porphyritic or micro-porphyritic basalt.|
2950|Bunbury Basalt|44303|4|Described|map, p.7,9,11,13,19||Early Cretaceous|Lower Cretaceous. (I/50-5,9).||||||
2950|Bunbury Basalt|60372|5|Briefly described|p85 Fig.1.|Early Cretaceous|Early Cretaceous|Also presented as Bunbury basalt and (throughout the article) Bunbury basalts. Linked to opening of the Indian Ocean.|132-123 Ma.|||||06-FEB-18
2950|Bunbury Basalt|60386|5|Briefly described|p302|Aptian|Hauterivian|Perth Basin.|123,130, 136 Ma|||||
2950|Bunbury Basalt|60556|5|Briefly described|p23, p24, p25 Fig. 15|||||||||
2950|Bunbury Basalt|60638|6|Mentioned|p234 Fig. 8|||||||||
2950|Bunbury Basalt|61023|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|||||||
2950|Bunbury Basalt|64580|4|Described|map legend||Early Cretaceous|Porphyritic and micro-porphyritic basalt in multiple flows, minor associated dolerite and basalt sills.||||||09-DEC-08
2950|Bunbury Basalt|64769|5|Briefly described|p34, p36 Fig. 25, p129, p130 Fig. 133|Cretaceous|Cretaceous|Underlain by Yarragadee Formation. Black and columnar basalt. WA.||||||05-MAY-09
2950|Bunbury Basalt|65269|6|Mentioned|p38|||Used as an internal reference material by GSWA for geochemical analyses||||||
2950|Bunbury Basalt|65306|5|Briefly described|p20, p21 (fig)|||Unconformably overlies the Yarragadee Formation and its aquifer.||||||10-SEP-09
2950|Bunbury Basalt|65506|6|Mentioned|p990-991|||Mentioned as GSWA internal reference material for geochemical analysis.||||||
2950|Bunbury Basalt|67135|6|Mentioned|p8, p52, p53.|||A valuable source of high-quality aggregate in Bunbury region. Has economic potential as cobbles and setts and as black, polished blocks.||||||
2950|Bunbury Basalt|67888|6|Mentioned|p49|||||||||
2950|Bunbury Basalt|67925|5|Briefly described|Ch1 p33, Ch3 p8, Ch4 p8 fig 2|Upper Jurassic|Upper Jurassic|Produces visible anomalies in magnetic data from this report. ||||Unconformably overlies the Yarragadee Formation. Unconformably overlain by the Warnbro Group and the Leederville Formation.||
2950|Bunbury Basalt|68193|5|Briefly described|p5|Cretaceous|Cretaceous|Associated with the break-up of Gondwana.|132 Ma (Zhu et al., 2009).|||||
2950|Bunbury Basalt|68811|5|Briefly described|p97, p98 fig 56|Cretaceous|Cretaceous|Hosts an aquifer in the Bunbury area.||||Overlies the Yarragadee Formation.||15-APR-20
2950|Bunbury Basalt|69182|6|Mentioned|Ch2 p3|Cretaceous|Cretaceous|Perth Basin. See also Ch2 p52-p53, Ch2 p55, Ch2 p57, Ch2 p60-p63, Ch2 p84-p86||||Overlies the Parmelia Group. Overlain by the South Perth Shale.||
2950|Bunbury Basalt|69297|6|Mentioned|p175, p189|Hauterivian|Berriasian|Vlaming Sub-basin, South Perth Basin. ||||Overlies the Parmelia Group. Overlain by the Gage Sandstone and the South Perth Shale.||
2950|Bunbury Basalt|70097|5|Briefly described|p19 Fig.3|Valanginian|Valanginian|Southern Perth Basin. Bunbury Trough.||Warnbro Group|||Basalt.|
2950|Bunbury Basalt|70099|6|Mentioned|Fig.4|Hauterivian|Berriasian|||||Overlies Parmelia Group. Is overlain by Warnbro Group.||
2950|Bunbury Basalt|70128|6|Mentioned|p453|||Perth Basin.||||||
2950|Bunbury Basalt|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Perth Basin.||||||
2950|Bunbury Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt|
2950|Bunbury Basalt|71377|5|Briefly described|p7|Early Cretaceous|Early Cretaceous|Perth Basin.||Warnbro Group||||
2950|Bunbury Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Aptian|Hauterivian|Perth Basin.|132+/-1 Ma max, 123+/-2 min||||Porphyritic and microporphyritic basalt in multiple flows; minor dolerite and basalt sills.|
2950|Bunbury Basalt|72251|6|Mentioned|p56|||||||||
2950|Bunbury Basalt|72258|5|Briefly described|p129-131,133,135,138|Early Cretaceous|Early Cretaceous|Of Perth Basin. Eruptive basaltic lavas onto a breakup unconformity during continental breakup (breakup of India and Australia-Antarctica; Gibbons et al., 2012; Jones et al., 2012) within N-S striking Bunbury Trough. Comprises three distinct lava flows into two deeply-incised axially-draining paleovalleys.|137-130 Ma |||Overlain unconformably by Leederville Formaton or Gage Sandstone. Underlain unconformably by Parmelia Group.||
2950|Bunbury Basalt|73424|6|Mentioned|p3|||||||||
2950|Bunbury Basalt|73480|6|Mentioned|p203, p215 Fig.10, p218|Early Cretaceous|Early Cretaceous||ca 137-130 Ma|||||
2950|Bunbury Basalt|73598|6|Mentioned|p1210|||Used as a geochemical reference.||||||
3005|Bungarra Member|41199|4|Described|p12|||Reserved as Bungarra. Of Menzies Formation.||||||
3056|Burbanks Formation|24139|5|Briefly described|p239 Table 1|||Geological Province: Coolgardie Domain.  Of the Coolgardie Group.||||||
3056|Burbanks Formation|42221|6|Mentioned|Table 1 P6|||||||||
3056|Burbanks Formation|42696|6|Mentioned|Plate 1B|||||||||
3056|Burbanks Formation|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
3056|Burbanks Formation|42892|5|Briefly described|Fig.27|||of Coolgardie Group||||||
3056|Burbanks Formation|43102|6|Mentioned|p9|||||||||
3056|Burbanks Formation|43125|6|Mentioned|Table 1|||||||||03-MAR-10
3056|Burbanks Formation|43162|6|Mentioned|5|||||||||
3056|Burbanks Formation|43496|6|Mentioned|6|||||||||
3056|Burbanks Formation|60514|6|Mentioned|p65 Table 1.|Archean|Archean|Of the Coolgardie Group. Geological Province: Coolgardie Domain, Yilgarn Craton.||||||07-FEB-11
3056|Burbanks Formation|60627|5|Briefly described|p65 Tb.1|||Of Coolgardie Group.||||||
3056|Burbanks Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|Coolgardie Domain.  Kambalda Sequence.|||||Tholeiitic and high MgO basalt.|
3056|Burbanks Formation|65204|6|Mentioned|p11|||S of Coolgardie. Coarsely plagioclase-phyric basalt, similar to Victorious Basalt.||||||
3056|Burbanks Formation|65834|6|Mentioned|p7|||Coolgardie Domain, Kalgoorlie Terrane.||Coolgardie Group.||||
3056|Burbanks Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2726 - 2699 Ma (inferred).|Coolgardie Subgroup|Includes Little Blow Member||Tholeiitic basalt; massive, vesicular to porphyritic; variably foliated; includes rare ultramafic and sedimentary rocks; intruded by thin dolerite sills; metamorphosed.|
3056|Burbanks Formation|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2726-2699 Ma (inferred)|Unit of Coolgardie Subgroup.|Includes Little Blow Member.|Intruded by Tindals Diorite.|Tholeiitic basalt; massive, vesicular to porphyritic; variably foliated; includes rare ultramafic and sedimentary rocks; intruded by thin dolerite sills; metamorphosed|
3056|Burbanks Formation|73391|6|Mentioned|Appendices.|||Hunter (1993). Regional stratigraphic correlation chart of other workers. See Burbanks Basalt (p194, 244, Appendices).|||||High-Mg basalt flows, minor mafic intrusions, shale, and tholeiitic flows, porphyritic basalt-dolerite.|
3056|Burbanks Formation|73596|6|Mentioned|p1162|||Coolgardie Inlier, Kalgoorlie Terrane.||||Is overlain by Greenmont Basalt.||
3168|Burt Range Formation|13194|4|Described|p390 Tb. 4-16, p402 fig 4-66|Early Tournaisian|Early Tournaisian|Type Section: Burt Range 15o38'S 128o55'E. 220-460m thick marine shelf to shoreface deposits.||Langfield Group||Overlies Buttons Formation (conformably), Djilirri Limestone (unconformably). Overlain by Enga Sandstone (conformably).|Limestone, sandy limestone, minor sandstone.|
3168|Burt Range Formation|13234|5|Briefly described|p252|||Includes traces of oil.||||||27-OCT-14
3168|Burt Range Formation|23820|5|Briefly described|p203|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
3168|Burt Range Formation|31519|6|Mentioned|p917|||||||||
3168|Burt Range Formation|32469|6|Mentioned|p533|||||||||
3168|Burt Range Formation|32648|6|Mentioned|p32|||Tournaisian||||||
3168|Burt Range Formation|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
3168|Burt Range Formation|32699|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Limestone, minor shale and sandstone.||||||02-DEC-04
3168|Burt Range Formation|32701|4|Described|Table 2|||L.Carb. See also p15.||||||02-AUG-06
3168|Burt Range Formation|32865|6|Mentioned|p475|||||||||
3168|Burt Range Formation|32867|6|Mentioned|p47|||||||||
3168|Burt Range Formation|32870|6|Mentioned|p46|||Refers Veevers, Roberts (1968)||||||
3168|Burt Range Formation|33621|6|Mentioned|Table 1|||Tournaisian||||||
3168|Burt Range Formation|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
3168|Burt Range Formation|34155|6|Mentioned|p93|||||||||
3168|Burt Range Formation|36257|6|Mentioned|Table 2.1|||||||||
3168|Burt Range Formation|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
3168|Burt Range Formation|36551|6|Mentioned|Table 16|||||||||
3168|Burt Range Formation|36890|3|Fully described|p379|||Formerly Burt Range Series. Includes Spirit Hill Limestone.||||||02-AUG-06
3168|Burt Range Formation|36904|5|Briefly described|p9|||||||||
3168|Burt Range Formation|38277|6|Mentioned|p149|||||||||
3168|Burt Range Formation|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
3168|Burt Range Formation|40494|4|Described|p16|||||||||
3168|Burt Range Formation|40792|6|Mentioned|p173|||||||||
3168|Burt Range Formation|40993|6|Mentioned|p10|||||||||
3168|Burt Range Formation|41023|6|Mentioned|p289|||||||||
3168|Burt Range Formation|41598|6|Mentioned|p412|||||||||
3168|Burt Range Formation|41712|6|Mentioned|p285|||||||||
3168|Burt Range Formation|41731|6|Mentioned|Table 1|||||||||
3168|Burt Range Formation|41839|4|Described|p27|||Formerly "Burt Range Series", "Burt Range Limestone"||||||
3168|Burt Range Formation|41864|3|Fully described|p101|||Formerly "Burt Range Series", "Burt Range Limestone"||||||
3168|Burt Range Formation|41865|5|Briefly described|Map legend|middle Tournaisian|early Tournaisian|||||||
3168|Burt Range Formation|41867|5|Briefly described|Map legend|middle Tournaisian|early Tournaisian|||||||
3168|Burt Range Formation|42175|5|Briefly described|p197|||||||||
3168|Burt Range Formation|42547|4|Described|p98|||||||||
3168|Burt Range Formation|42933|5|Briefly described|Fig.94 p258|||||||||
3168|Burt Range Formation|42994|6|Mentioned|p28|||||||||
3168|Burt Range Formation|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
3168|Burt Range Formation|44994|6|Mentioned|p14|||L.Carb. See also Fig.6.||||||
3168|Burt Range Formation|45038|2|Defined|p.66||Early Carboniferous|See also Plates & Figs.||||||
3168|Burt Range Formation|45039|4|Described|p1|||See also pp5-8,14 etc. Lower Carboniferous.||||||02-AUG-06
3168|Burt Range Formation|45040|14|Not recorded|p4||Early Carboniferous|See also p7,8,10,12,14,62,73, Fig. 2,7. L.Carboniferous.||||||
3168|Burt Range Formation|45050|6|Mentioned|p46|||See also pp57,59,60,77.||||||02-AUG-06
3168|Burt Range Formation|45056|6|Mentioned|p8|||Tournaisian Fig.3.||||||
3168|Burt Range Formation|45063|6|Mentioned|p7|||See also p14, 29 & Fig. 3. L.Carb.||||||02-AUG-06
3168|Burt Range Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
3168|Burt Range Formation|45133|6|Mentioned|Fig.13|||||||||
3168|Burt Range Formation|45169|4|Described|p4|||||||||
3168|Burt Range Formation|47040|6|Mentioned|p150|||||||||
3168|Burt Range Formation|48635|14|Not recorded|p.1,5,7-12,17,20-22||Early Carboniferous|Pl.1, Sh.4, Pl.2, Sh.3. Lower Carboniferous. Fig.1.||||||
3168|Burt Range Formation|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
3168|Burt Range Formation|48971|6|Mentioned|p15,3,33,37,40,42|||||||||
3168|Burt Range Formation|48978|6|Mentioned|p4|||Analysis Appendix III.||||||
3168|Burt Range Formation|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Of Langfield Group. Calcareous sandstone, quartzic limestone, dolostone.||||||23-JUL-04
3168|Burt Range Formation|60364|4|Described|p184, 187, 192|Tournaisian|Tournaisian|Disconformably overlies Buttons Formation. Overlain by Enga Sandstone or Border Creek Formation. Max. thickness: ~460m. Fossiliferous calcarenite grading up into calcareous quartz sandstone. Of Langfield Gp. Geological Province: Bonaparte Basin.||||||11-MAY-05
3168|Burt Range Formation|60682|5|Briefly described|piii, p22 Table 5, p23|Tournaisian|Tournaisian|Of Langfield Group. Disconformably overlies Cockatoo Group. Conformably overlain by Enga Sandstone. Max. Thickness: >400m. Geological Province: Bonaparte Basin.||||||
3168|Burt Range Formation|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
3168|Burt Range Formation|64159|5|Briefly described|p93|Early Carboniferous|Early Carboniferous|Of the Langfield Group. Geological Province: Bonaparte Basin. Prospective rocks comprise a succession of dolomitised shelf, marginal marine and tidal deposits.||||||03-JUN-08
3168|Burt Range Formation|64580|6|Mentioned|map legend|||Of Langfield Group.||||||15-DEC-08
3168|Burt Range Formation|64694|5|Briefly described|p232, p233, p234, p237-239, p240|Tournaisian|Tournaisian|See also p241, p247, p252, p254 Fig.12. Carlton Shelf, Onshore Bonaparte Basin. Appears inexplicably as Upper and Lower Burt Range Formation on p240.||Basal unit in Langfield Group.|Includes Gooseneck, Sorby Dolomite, Knox Siltstone, Members.|||
3168|Burt Range Formation|65331|5|Briefly described|Map legend|Tournasian|Tournasian|Of Langfield Group, Bonaparte Basin. Informally subdivided. Calcareous sandstone, quartzic limestone, dolostone, dolarenite, leached carbonate, siltstone, silty dolostone, quartzic dolostone. ||||||
3168|Burt Range Formation|65342|5|Briefly described|p14. |||Bonaparte Basin. Max. thickness at least 125 m.||||Is overlain by Enga Formation.|Calcarenite grading into sandstone.|
3168|Burt Range Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes heterolithic fine-grained cream sandstone and greenish grey siltstone.|
3168|Burt Range Formation|67200|5|Briefly described|app 2 p8||||||||Heterolithic fine grained sandstone and siltstone.|
3168|Burt Range Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||31-JUL-15
3168|Burt Range Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||
3168|Burt Range Formation|69418|6|Mentioned|p3:11|||Bonaparte Basin. Hosts Pb-Zn-Ag deposits (described).||||||12-JUL-16
3168|Burt Range Formation|69452|4|Described|p36:6, 9, 12-13, 23-26|Tournaisian|Tournaisian|Veevers and Roberts (1968). Equivalent to Burt Range Limestone of Noakes et al. (1952). Petrel Sub-basin, Bonaparte Basin. Inner shelf to shoreface deposits on a clastic-influenced carbonate platform. Up to 460m thick. Onshore. Hosts numerous Zn/Pb occurrences including Sandy Creek Pb-Zn-Ag deposit in NT (described in detail), and the significant Sorby Hills Ag-Pb-Zn deposit in WA. Local ochre deposits.||Langfield Group.||Disconformably overlies Ningbing Group. Is overlain conformably (locally unconformably) by Enga Sandstone, and probably unconformably by Milligans Formation. Is faulted against Kellys Knob Sandstone.|Calcareous sandstone, quartzose limestone and dolostone, minor carbonaceous shale. A diverse fossil assemblage.|12-JUL-16
3168|Burt Range Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Unit of Langfield Group.||||
3168|Burt Range Formation|69673|5|Briefly described|p171, p180|||460m thick. (In WA)|||||Calcareous sandstone, quartzic limestone, dolostone and carbonaceous shale.|
3168|Burt Range Formation|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin. Includes two unnamed members: calcareous sandstone, dolarenite, leached carbonate rocks;  quartzic limestone, siltstone, silty dolostone, upper quartzic dolostone.||Langfield Group|Includes two unnamed members.||Calcareous sandstone, quartzic limestone, dolostone.|
3168|Burt Range Formation|70812|5|Briefly described|p19|Lower Carboniferous|Lower Carboniferous|Bonaparte Basin. Hosts the Sorby Hills deposits.|||||Carbonates.|
3168|Burt Range Formation|71146|6|Mentioned|p27|Lower Carboniferous|Lower Carboniferous|Southern Bonaparte Basin. Hosts 13 irregular minerlized bodies across an 8km trend.||||||
3168|Burt Range Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Calcareous sandstone, quartzic limestone, dolostone, shale|
3187|Burvill Formation|13194|4|Described|p389 Tb. 4-16, p402 fig 4-66|Upper Carboniferous|Visean|Type Section: Burvill Point 15o16'S 128o41'S. 50-90m thick prodeltaic deposits.||Weaber Group||Overlies Milligans Formation, Utting Calcarenite, Waggon Creek Formation (all conformably).|Sandstone, minor limestone, siltstone and mudstone.|
3187|Burvill Formation|24390|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
3187|Burvill Formation|40993|6|Mentioned|Fig.1|||||||||
3187|Burvill Formation|41532|6|Mentioned|Fig.15|||||||||
3187|Burvill Formation|41839|4|Described|p31|||Formerly "Burvill Beds"||||||
3187|Burvill Formation|41864|3|Fully described|p130|||||||||
3187|Burvill Formation|41865|5|Briefly described|Map legend|Namurian|late Visean|||||||
3187|Burvill Formation|41867|5|Briefly described|Map legend|Namurian|late Visean|||||||
3187|Burvill Formation|42442|6|Mentioned|p11|||Variation of Burvill Formation, WA.||||||
3187|Burvill Formation|42547|4|Described|p102|||||||||
3187|Burvill Formation|50085|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
3187|Burvill Formation|60006|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Bonaparte Basin. Of the Weaber Group. Sandstone, siltstone, shale, calcareous sandstone, quartzic limestone.||||||
3187|Burvill Formation|60364|4|Described|p186 Fig.3|Visean|Visean|Conformably overlies Utting Calacarenite and Milligans Formation. Conformably overlain by Point Spring Sandstone. Coarse ferruginous quartz sandstone and interbedded sandy limestone. Max. thickness: 85m. Geological Province: Bonaparte Basin.||||||
3187|Burvill Formation|60682|4|Described|p22 Table 5, p25|Namurian|Visean|Of Weaber Group. Conformably overlies Milligans Formation, laterally equivalent to lower Tanmurra Formation. Conformably overlain by Point Spring Sandstone. Formally known as Burvill beds. Max. thickness: <80m. Geological Province: Bonaparte Basin.||||||11-MAY-05
3187|Burvill Formation|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||10-APR-08
3187|Burvill Formation|61542|5|Briefly described|p276, p277 Fig. 2, p285|Visean|Visean|Of the Weaber Group. Overlies Yow Creek Formation (formerly Milligans Fm.). Geological Province: Bonapart Basin/Petrel-Sub-basin. Sandstone, minor siltstone, shale and limestone; contains brachiopods.||||||07-FEB-11
3187|Burvill Formation|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
3187|Burvill Formation|64694|6|Mentioned|p232, p234, p238 Tb.1|||Carlton Shelf, Onshore Bonaparte Basin.||Unit in Weaber Group.||Is overlain by Point Spring Sandstone.||
3187|Burvill Formation|65331|5|Briefly described|Map legend|Visean|Visean|Of Bonaparte Basin. Of Weaber Group. Sandstone, siltstone, shale, calcareous sandstone, quartzic limestone ||||||
3187|Burvill Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
3187|Burvill Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
3187|Burvill Formation|69452|4|Described|p36:9, 12, 14, 16|Early Carboniferous|Early Carboniferous|Cockbain (1985). Equivalent to the Burvill Beds of Veevers and Roberts (1968) and Burvill beds of Jones (1984). Petrel Sub-basin, Bonaparte Basin. Lower shoreface and offshore delta front or prodelta deposits. Up to 80m thick. Onshore (subsurface) in NT, but crops out in Carlton Sub-basin in WA. Late Visean to possibly early Namurian age.||Weaber Group.||Overlies Milligans Formation (?Yow Creek Formation) conformably. Lateral equivalent of Utting Calcarenite and Kingfisher Shale. Is overlain unconformably by Tanmurra Formation.|Sandstone, typically fine- to very fine-grained; minor siltstone, shale, calcareous sandstone and quartzose limestone. A diverse assemblage of macrofossils, trace and microfossils.|12-JUL-16
3187|Burvill Formation|69673|6|Mentioned|p168 fig 139, p172|Carboniferous|Carboniferous||||||Sandstone and minor siltstone, shale, calcareous sandstone and quartzic limestone.|
3187|Burvill Formation|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Weaber Group|||Sandstone, siltstone, shale, calcareous sandstone, quartzic limestone.|
3187|Burvill Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Weaber Group.|||Sandstone, siltstone, shale, calcareous sandstone, quartzic limestone|
3187|Burvill Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by and equivalent to Utting Calcarenite. Equivalent to Kingfisher Shale. Overlain by Tanmurra Formation.||
3230|Byro Group|12466|5|Briefly described|p178.|Permian|Permian|Enderby Terrace, Dampier Sub-basin. No demonstrated hydrocarbon source potential.|||||Sandstones and claystones.|
3230|Byro Group|12731|6|Mentioned|p596 Fig.9.|||||||Overlies Wooramel Group.||
3230|Byro Group|12733|5|Briefly described|p554 Fig.2, pp565-566.|Early Permian|Early Permian|Artinskian. Gaseous source in Merlinleigh Sub-basin.|||Includes Quinnanie and Bulgadoo Shales.|Overlies Wooramel Group. Is overlain by Kennedy Group.|Predominantly clastic shallow marine deposits.|
3230|Byro Group|13615|5|Briefly described|p17, 41, 55, 58, 62, p103 App.3|Early Permian|Early Permian|Peedamullah Shelf.|||Includes the Wandagee Limestone.|Conformably overlain by Kennedy Group.||07-FEB-19
3230|Byro Group|14228|4|Described|p1, p5 Fig.2, p8-10, p15-18, p20-21|Lower Permian|Kungurian|Petroleum source beds. About 1500m thick. Deposition > 300m/my on stormy shelf. Intruded by Jurassic alkali picrite diatremes and sills.|||Includes Coyrie, Cundlego, Wandagee and Baker Formations; Mallens and Nalbia Sandstones; Bulgadoo and Quinnanie Shales.|Overlies Wooramel Group conformably. Overlain by Kennedy Group.|Carbonaceous siltstone and mudstone alternating with fine-grained, commonly bioturbated sandstone.|
3230|Byro Group|22814|5|Briefly described|fig2|Permian|Permian|||||||
3230|Byro Group|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
3230|Byro Group|23311|5|Briefly described|map legend|Artinskian|Artinskian|||||||
3230|Byro Group|23312|5|Briefly described|map legend|Artinskian|Artinskian|||||||
3230|Byro Group|23403|4|Described|p7|Late Permian|Middle Devonian|||||||24-NOV-09
3230|Byro Group|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Includes Coyrie Formation.||||||
3230|Byro Group|23574|5|Briefly described|Map Legend|Early Permian|Early Permian|Underlying unit Wooramel Group.||||||
3230|Byro Group|23576|5|Briefly described|Map Legend|Early Permian|Early Permian|Underlying unit Wooramel Group.||||||
3230|Byro Group|23577|5|Briefly described|Map Legend|Early Permian|Early Permian|Underlying unit Wooramel Group.||||||
3230|Byro Group|23620|5|Briefly described|p4 Fig. 4|Permian|Permian|||||||
3230|Byro Group|23726|4|Described|p37|Late Permian|Early Permian|Overlying unit Kennedy Group. Underlying unit Wooramel Group. Geological Province: Carnarvon Basin.||||||
3230|Byro Group|23815|4|Described|p281, 284, 288|Artinskian|Artinskian|Geological Province: Carnarvon Basin. Contains the Newman Subgroup (uppermost unit) and the Minilya Subgroup (lowermost unit). Overlying unit: Kennedy Group (disconformable).||||||18-APR-05
3230|Byro Group|23976|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
3230|Byro Group|23977|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
3230|Byro Group|23978|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
3230|Byro Group|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|||||||
3230|Byro Group|24059|5|Briefly described|p130|Permian|Permian|Geological Province: Barrow Sub-basin.||||||
3230|Byro Group|24114|5|Briefly described|p5 Fig.4|||Geological Province: Carnarvon Basin.||||||
3230|Byro Group|24331|5|Briefly described|p475 Fig.2|Permian|Permian|Unconformably overlain by the Chinty Formation. Marine to marginal marine. Geological Province: Barrow Sub-basin.||||||
3230|Byro Group|24390|5|Briefly described|p19 Fig. 10||Permian|Geological Province: Southern Carnarvon Basin.||||||
3230|Byro Group|24410|5|Briefly described|p137 Fig. 80|Permian|Permian|Sandstone, siltstone and shale - fine-grained, locally fossiliferous, shelf sequence consisting of bioturbated siltstone and silty sandstone with fine-grained calcareous sandstone.||||||24-NOV-09
3230|Byro Group|29548|6|Mentioned|p225|||Permian||||||
3230|Byro Group|30545|6|Mentioned|p24|||In Byro Group. Lower Permian||||||
3230|Byro Group|30550|6|Mentioned|p94|||Fauna.||||||
3230|Byro Group|31251|6|Mentioned|p68|||Refers Thomas (1958) & McWhae et al. (1958).||||||
3230|Byro Group|31396|6|Mentioned|p1183|||||||||
3230|Byro Group|31561|4|Described|p7|||See also p8-9, p32, p34. Hydrocarbon potential. Stratigraphy.||||||05-APR-19
3230|Byro Group|31604|6|Mentioned|p6|||See also Table 4. Artinskian||||||
3230|Byro Group|32113|6|Mentioned|p47|||||||||
3230|Byro Group|32648|6|Mentioned|p32|||L.Perm.||||||
3230|Byro Group|32945|6|Mentioned|p88|||See also P89. Permian.||||||
3230|Byro Group|32979|6|Mentioned|p38|||Correlation with basins in India||||||
3230|Byro Group|33386|6|Mentioned|Fig.7|||||||||
3230|Byro Group|33450|6|Mentioned|Fig.5|||||||||
3230|Byro Group|33453|6|Mentioned|p70|||Artinskian-Tatarian.||||||
3230|Byro Group|33701|6|Mentioned|Fig.1|||Kungurian & Artinskian.||||||
3230|Byro Group|33710|4|Described|p120|||||||||
3230|Byro Group|33711|6|Mentioned|p384|||See also Table 4.||||||
3230|Byro Group|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
3230|Byro Group|34532|6|Mentioned|p225|||||||||
3230|Byro Group|34721|6|Mentioned|p286|||||||||
3230|Byro Group|34846|6|Mentioned|Fig.3|||||||||
3230|Byro Group|35144|6|Mentioned|Fig.5|||||||||
3230|Byro Group|35282|6|Mentioned|Fig.2|||||||||
3230|Byro Group|36020|6|Mentioned|p392|||||||||
3230|Byro Group|36208|6|Mentioned|p253|||||||||
3230|Byro Group|36257|6|Mentioned|Table 2.1|||||||||
3230|Byro Group|36890|3|Fully described|p283|||Formerly Byro Limestone Group, Byro Formation.||||||11-APR-08
3230|Byro Group|36899|6|Mentioned|p1091|||||||||
3230|Byro Group|37000|6|Mentioned|p23|||||||||
3230|Byro Group|37294|6|Mentioned|p100|||||||||
3230|Byro Group|37295|4|Described|p54|||See also p51.||||||05-APR-19
3230|Byro Group|37303|6|Mentioned|Table 1|||||||||
3230|Byro Group|37304|4|Described|p55|||||||||
3230|Byro Group|37812|6|Mentioned|p653|||||||||
3230|Byro Group|37920|6|Mentioned|p457|||||||||
3230|Byro Group|38444|6|Mentioned|p300|||||||||
3230|Byro Group|38493|4|Described|p35|||||||||
3230|Byro Group|38494|6|Mentioned|p19|||||||||
3230|Byro Group|38917|6|Mentioned|p168|||See also P171||||||
3230|Byro Group|38998|6|Mentioned|p34|||||||||
3230|Byro Group|39263|6|Mentioned|p152|||||||||
3230|Byro Group|39316|6|Mentioned|Fig.2|||||||||
3230|Byro Group|39427|4|Described|Table 1|||||||||
3230|Byro Group|40336|6|Mentioned|p18|||||||||
3230|Byro Group|40339|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
3230|Byro Group|40340|6|Mentioned|p20|||||||||
3230|Byro Group|40343|5|Briefly described|p11|||||||||
3230|Byro Group|40395|6|Mentioned|p334|||||||||
3230|Byro Group|40617|6|Mentioned|Fig.1|||||||||
3230|Byro Group|40992|6|Mentioned|Fig.8|||||||||
3230|Byro Group|41158|5|Briefly described|p231|||||||||
3230|Byro Group|41170|6|Mentioned|Fig.4|||||||||
3230|Byro Group|41172|6|Mentioned|p123|||||||||
3230|Byro Group|41271|3|Fully described|p90|||||||||
3230|Byro Group|41436|6|Mentioned|p42|||||||||
3230|Byro Group|41438|4|Described|p104|||||||||
3230|Byro Group|41440|4|Described|p133|||||||||
3230|Byro Group|41441|5|Briefly described|p151|||||||||
3230|Byro Group|41443|6|Mentioned|p163|||||||||
3230|Byro Group|41444|6|Mentioned|Fig.4|||||||||
3230|Byro Group|41446|6|Mentioned|Fig.17|||||||||
3230|Byro Group|41447|6|Mentioned|Fig.3|||||||||
3230|Byro Group|41689|6|Mentioned|Table 1|||||||||
3230|Byro Group|42116|4|Described|p27|||See also Fig.11||||||
3230|Byro Group|42392|6|Mentioned|p115|||||||||
3230|Byro Group|42462|6|Mentioned|p55|||||||||
3230|Byro Group|42473|6|Mentioned|p9|||||||||
3230|Byro Group|42711|6|Mentioned|p30|||Geological province: Carnarvon Basin.  Shallow marine deposits.||||||
3230|Byro Group|42994|6|Mentioned|p53|||||||||
3230|Byro Group|43018|5|Briefly described|Table 1,p386|||||||||
3230|Byro Group|43050|5|Briefly described|p7|||||||||
3230|Byro Group|43255|5|Briefly described|map legend||Artinskian|||||||
3230|Byro Group|43256|5|Briefly described|5-22||Permian|||||||24-NOV-09
3230|Byro Group|43474|14|Not recorded|p26|||||||||
3230|Byro Group|43564|6|Mentioned|p445||Permian|||||||
3230|Byro Group|43580|6|Mentioned|p361|||||||||
3230|Byro Group|43712|5|Briefly described|p10||Permian|||||||
3230|Byro Group|43722|5|Briefly described|p9||Permian|||||||
3230|Byro Group|43724|5|Briefly described|p28||Permian|||||||
3230|Byro Group|43826|6|Mentioned|Fig.2,p163||Late Permian|||||||01-MAR-10
3230|Byro Group|43835|5|Briefly described|Map Legend||Artinskian|||||||
3230|Byro Group|43882|14|Not recorded|p95||Early Permian|Correlated with middle part of Middle Bowen Beds (Gebbie Formation)||||||
3230|Byro Group|44219|14|Not recorded|p31|Kungurian|Artinskian|||||||
3230|Byro Group|44344|14|Not recorded|p.3,10,11-15||Permian|Contains Minilya & Newman Subgroups (q.v.). (G50-1). opp.4,map.||||||
3230|Byro Group|44345|14|Not recorded|map legend||Artinskian|||||||
3230|Byro Group|44532|4|Described|p.7, map|||(G50-5).||||||
3230|Byro Group|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
3230|Byro Group|44537|14|Not recorded|map legend||Artinskian|||||||
3230|Byro Group|44657|14|Not recorded|p.9|||||||||
3230|Byro Group|44994|6|Mentioned|Fig.7|||Correlation.||||||
3230|Byro Group|45001|14|Not recorded|p7,p146|Kungurian|Artinskian|Includes Madeline Formation at base.||||||25-NOV-16
3230|Byro Group|45015|5|Briefly described|map legend|Artinskian|Artinskian|Comprises the Newman and Minilya Sub-Groups.||||||01-JUN-06
3230|Byro Group|45016|2|Defined|p.122-126||Artinskian|Tb at back, p.12,19,57,74,75,79,82,88,91,98,118,121,138,144,155,170,174,176,179. (F50-9,13,G50-1,2,5,6,9,10).||||||
3230|Byro Group|46849|6|Mentioned|p186|||||||||
3230|Byro Group|47041|6|Mentioned|p166|||||||||
3230|Byro Group|48610|4|Described|p4|||||||||
3230|Byro Group|48615|6|Mentioned|Fig.4|||(F50-13/Wandagee).||||||
3230|Byro Group|48628|14|Not recorded|Figs.2,5|||(F50-13/Wandagee).||||||
3230|Byro Group|48831|14|Not recorded|p.15-17|||On many pages. p.15-17,22,31,32,37,63.||||||
3230|Byro Group|48848|14|Not recorded|p.35,38,43,64,80-84|||||||||
3230|Byro Group|48857|14|Not recorded|p.15|||||||||
3230|Byro Group|48858|14|Not recorded|p.1-15|||(G50-1/Norton). Pl.1,2.||||||
3230|Byro Group|48861|2|Defined|p.1,5,8|||Pl.1.||||||
3230|Byro Group|48885|14|Not recorded|p.5,10|||(G/50-6).||||||
3230|Byro Group|49644|5|Briefly described|Table|||||||||
3230|Byro Group|49942|5|Briefly described|p5|Permian|Permian|Geological Province: Gascoyne Platform.||||||
3230|Byro Group|50085|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
3230|Byro Group|60331|5|Briefly described|p33 Fig.2|Kungurian|Artinskian|Overlain by the Kennedy Group. Overlies the Wooramel Group. Geological Province: Southern Carnarvon Basin.||||||04-MAY-05
3230|Byro Group|60386|5|Briefly described|p297, 311|Kungurian|Kungurian|Carnarvon Basin. Limestone nearshore-shelf. Storm deposits and fine-grained siliciclastics. ||||||
3230|Byro Group|60725|5|Briefly described|p29-32, p34, p36.|Early Permian|Early Permian|Carnarvon Basin. Good to fair predominantly gas-generating source rock intervals are present.||||||10-MAY-17
3230|Byro Group|61023|5|Briefly described|p34 Fig. 14|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
3230|Byro Group|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Includes the Newman and Minilya Sub-groups.||||||
3230|Byro Group|64580|4|Described|map legend||Early Permian|Siltstone, shale, sandstone; includes COYRIE FORMATION, MALLENS SANDSTONE, BULGADOO SHALE, CUNDLEGO FORMATION, QUINNANIE SHALE, WANDAGEE FORMATION, NALBIA SANDSTONE, and BAKER FORMATION. ||||||
3230|Byro Group|64630|5|Briefly described|p31 Fig.2, p35|Kungurian|Artinskian|Province: Southern Carnarvon Carnavon Basin. Underlies the Kennedy Group, overlies the Wooramel Group. Includes Coyrie Formation at base. Palynology age: M. trisina to P. sinuosis. Roughly correlates with the Carynginia Formation.||||||18-JAN-10
3230|Byro Group|64972|6|Mentioned|p615, p617 Fig. 4, p617 Fig. 5|Early Permian|Early Permian|Geological Province: Carnarvon Basin.||||||
3230|Byro Group|64974|6|Mentioned|p145, p146|Kungurian|Artinskian|Geological Province: Carnarvon Basin.||||||24-JUN-09
3230|Byro Group|64977|6|Mentioned|p493 Fig.3.|Permian|Permian|Thevenard Island area.||||||
3230|Byro Group|66189|6|Mentioned|p454, p455 Fig.2|Kungurian|Artinskian|Overlies the Wooramel Group; is overlain by Coolkinya Sandstone (Kennedy Group).||||||
3230|Byro Group|66579|5|Briefly described|Map legend|Permian|Permian|Southern Carnarvon Basin.|||Includes Coyrie Formation and Mallens Sandstone.||Sandstone, siltstone, black shale.|
3230|Byro Group|67200|6|Mentioned|p7 fig 5, p47, p54|Kungurian|Artinskian||||Includes Coyrie Formation, Mallens Sandstone, Bulgadoo Shale, Cundlego Formation, Wandagee Formation, Nalbia Sandstone, Baker Formation, Madeline Formation|Overlies Wooramel Group, overlain by Kennedy Group||
3230|Byro Group|67370|6|Mentioned|p327.|Artinskian|Artinskian|Carnarvon Basin. Alpine glacial episodes in lowermost parts.||||||
3230|Byro Group|67977|5|Briefly described|p479, p481 Fig. 2||Kungurian|Geol. Prov: Southern Carnarvon Basin (Byro Sub-basin and Merlinleigh Sub-basin)||||overlies Wooramel Group||
3230|Byro Group|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Subdivided into upper, middle, and lower parts.|||Includes Baker Formation, Nalbia Sandstone, Wandagee Formation, Quinnanie Shale, Cundlego Formation, Bulgadoo Shale, Mallens Sandstone, and Coyrie Formation.|Underlain by the Wooramel Group.|Includes sandstone, siltstone, conglomerate, claystone, and shale.|
3230|Byro Group|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.|||Includes Bulgadoo Shale, Cundlego Formation, Quinnanie Shale, Wandagee Formation, Coyrie Formation, and Mallens Sandstone.||Includes interbedded black mudstone, siltstone, and fine-grained sandstone; fine-grained bioturbated sandstone overlying interbedded sandstone, siltstone, and mudstone.|
3230|Byro Group|69029|5|Briefly described|p313,323,326-328,333|Artinskian|Artinskian|Of onshore Carnarvon Basin. Thickness: 700m (intersected in Kennedy-1). Contains good to fair, predominantly gas-prone source rock intervals.||||Overlain by Kennedy Group. Underlain by Wooramel Group.||
3230|Byro Group|69166|5|Briefly described|geologyp_lut.csv|Kungurian|Artinskian||||Includes Coyrie Formation, Mallens Sandstone, Bulgadoo Shale, Cundlego Formation, Quinnanie Shale, Wandagee Formaiton, Nalbia Sandstone, Baker Formation||Interbedded mudstone, siltstone and fine grained sandstone and shale.|
3230|Byro Group|69182|6|Mentioned|Ch3 p3, Ch3 p8, Ch3 p10-p11|||Carnarvon Basin. See also Ch3 p15, Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p50, Ch3 p54, Ch3 p67-p69, Ch3 p73. ||||Overlies the Lyons Group.||
3230|Byro Group|69547|4|Described|p182,192,194,201|Kungurian|Artinskian|Southern Carnarvon Basin. Characterised by siliciclastic facies with prominent mud-sand cyclicity in lower part of the section. Dropstones in the basal part of the section indicate glaciation; brachipods higher up in the lower section indicate warming, reaching a maximum at the Bulgadoo-Cundlego boundary.|||Includes Cundlego, Bulgadoo, Mallens, Coryie and Billidee formations.|||
3230|Byro Group|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin.|||Wandagee, Baker, Cundlego, Coyrie Formations; Nalbia, Mallens Sandstones; Bulgadoo Shale.|||
3230|Byro Group|70774|5|Briefly described|p5 fig 3|Kungurian|Artinskian|Southern Carnarvon Basin.||||Overlies the Billidee Formation (Wooramel Group). Overlain by the Kennedy Group.||
3230|Byro Group|70795|6|Mentioned|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 2_5m_interpgeop15_lut.csv|283-272 Ma||Includes Baker Formation, Nalbia Sandstone, Wandagee Formation, Quinnanie Shale, Cundlego Formation, Bulgadoo Shale, Mallens Sandstone, Coyrie Formation||Interbedded siltstone and fine grained sandstone; shale.|
3230|Byro Group|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Southern Carnarvon Basin.||||||
3230|Byro Group|71146|5|Briefly described|p6,  p43 fig 33|Kungurian|Artinskian|Southern Carnarvon Basin.||||Overlies the Wooramel Group. Overlain by the Kennedy Group.|Mudstone.|
3230|Byro Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, shale, sandstone, siltstone|
3230|Byro Group|72505|5|Briefly described|p890|Roadian|Kungurian|Southern Carnarvon Basin. Correlates with the Microbaculispora trisina zone and the Praecolpatites sinuosus zones.||||Overlies the Wooramel Group. Overlain by the Kennedy Group.||
3230|Byro Group|72910|4|Described|p1, p4, p6, 11, 14, p17-20, p23-25.|Kungurian|Artinskian|Thickness up to 1500m. Shown as part of the Byro and Merlinleigh Sub-basins. A storm-dominated marine shelf environment is suggested. See also p38, which says this Group is Artinskian. Also p41. Intersected by Kennedy Range 1 well which penetrates the full section of this group.|||Includes Bulgadoo Shale, Coyrie Formation, Mallens Sandstone, Cundlego Formation, Quinnanie Shale, Wandagee Formation, Nalbia Sandstone, and Baker Formation.|Conformably overlies Wooramel Group. Laterally equivalent to Carynginia Formation.|Dark siltstone and a succession of carbonaceous siltstone and mudstone with fine-grained, hummocky cross-stratified and bioturbated sandstone.|18-FEB-21
3230|Byro Group|73117|6|Mentioned|p15|Kungurian|Artinskian|||||Underlain by Wooramel Group. Correlates to Carynginia Formation.||
3230|Byro Group|73623|5|Briefly described|p4|Cisuralian|Cisuralian|Merlinleigh Basin.||||Overlies Wooramel Group. Is overlain by Kennedy Group. Correlative of Carynginia Formation.||
3266|Cadda Formation|12758|5|Briefly described|p17, p3 Fig. 3|Middle Jurassic|Middle Jurassic|Composed of marine clastics and fossiliferous limestone. Confined to the northern and central parts of Perth Basin. Overlain by Yarragadee Formation; conformably overlies Cattamarra Coal Measures.  Max. thickness: 300m.  See also p8 Fig. 9.||||||13-DEC-07
3266|Cadda Formation|14227|5|Briefly described|p8, p10|Middle Jurassic|Middle Jurassic|Age: Aalenian to Bajocian. Overlies Cattamarra Coal Measures. Thin marine flooding deposits of silt and sand. See also Enclosure 2.||||||07-FEB-11
3266|Cadda Formation|23172|4|Described|Map Legend|Jurassic|Jurassic|||||||
3266|Cadda Formation|23279|4|Described|p25,27-9|Bajocian|Aalenian|||||||
3266|Cadda Formation|23520|5|Briefly described|p6 Fig. 4|Middle Jurassic|Middle Jurassic|Overlies and seals the Cattamurra Coal Measures; conformably underlies the Yarragadee Formation. See also p9.||||||21-JUL-09
3266|Cadda Formation|23578|5|Briefly described|p6|Jurassic|Jurassic|See also p19 Tb. 6||||||
3266|Cadda Formation|23579|5|Briefly described|Map Legend|||||||||
3266|Cadda Formation|23816|4|Described|p241|Bajocian|Bajocian|Age: Middle Bajocian. Geological Province: Perth Basin. Underlying unit: Cockleshell Gully Formation (conformable). Overlying unit: Yarragadee Formation. Max. thickness: 84 m. Fossiliferous.||||||21-JUL-09
3266|Cadda Formation|24058|5|Briefly described|p112|Middle Jurassic|Middle Jurassic|Geological Basin: Perth Basin.||||||
3266|Cadda Formation|24160|6|Mentioned|p94|||Perth Basin.|||||Shale, siltstone, sandstone and limestone.|
3266|Cadda Formation|24351|5|Briefly described|p38, Plate 3 (in pocket)|Jurassic|Jurassic|Volcanic unit. Geological Province: Houtman Sub-basin (of Perth Basin). May provide local seal (for oil). Log Houtman-1. Name written as Cadda Fm.||||||21-JUL-09
3266|Cadda Formation|24390|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
3266|Cadda Formation|24443|5|Briefly described|p31|Middle Jurassic|Middle Jurassic|Overlies Cattamarra Coal Measures. Overlain by Yarragadee Formation. Marine shale. Geological Province: Houtman Sub-basin.||||||13-DEC-07
3266|Cadda Formation|29382|6|Mentioned|Table10|||||||||
3266|Cadda Formation|29693|6|Mentioned|Fig.7|||||||||
3266|Cadda Formation|29721|6|Mentioned|p226|||||||||
3266|Cadda Formation|29790|6|Mentioned|p93|||||||||
3266|Cadda Formation|30963|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
3266|Cadda Formation|31238|6|Mentioned|Fig. 12A|||||||||
3266|Cadda Formation|31561|6|Mentioned|p25|||Middle Jurassic. Widespread marine incursion||||||
3266|Cadda Formation|31562|6|Mentioned|Fig. 3|||||||||
3266|Cadda Formation|31568|5|Briefly described|p18|||M. Jurassic||||||
3266|Cadda Formation|31910|3|Fully described|Table 1|||See also p21.||||||06-OCT-20
3266|Cadda Formation|32136|6|Mentioned|p46|||Middle Bajocian||||||
3266|Cadda Formation|32648|6|Mentioned|p32|||Mid. Jur.||||||
3266|Cadda Formation|32649|6|Mentioned|p24|||||||||
3266|Cadda Formation|32714|6|Mentioned|Fig.2|||||||||
3266|Cadda Formation|32979|6|Mentioned|p38|||Correlation with basins in India||||||
3266|Cadda Formation|33166|6|Mentioned|p66|||||||||
3266|Cadda Formation|33386|6|Mentioned|Fig.7|||||||||
3266|Cadda Formation|33627|6|Mentioned|p582|||||||||
3266|Cadda Formation|34134|6|Mentioned|p482|||Bajocian||||||
3266|Cadda Formation|34172|6|Mentioned|p53|||Bajocian||||||
3266|Cadda Formation|34841|6|Mentioned|p95|||||||||
3266|Cadda Formation|35152|6|Mentioned|p3|||||||||
3266|Cadda Formation|35282|6|Mentioned|Fig.6|||||||||
3266|Cadda Formation|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin||||||
3266|Cadda Formation|35653|6|Mentioned|p1094|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
3266|Cadda Formation|35968|6|Mentioned|Fig.8|||||||||
3266|Cadda Formation|35970|6|Mentioned|Table 12|||||||||
3266|Cadda Formation|35983|6|Mentioned|Table 26|||||||||
3266|Cadda Formation|36100|6|Mentioned|Fig.2|||||||||
3266|Cadda Formation|36257|6|Mentioned|Table 2.1|||||||||
3266|Cadda Formation|36265|5|Briefly described|Fig.3.26|Middle Jurassic|Middle Jurassic|Geological Province: Perth Basin.||||||10-APR-08
3266|Cadda Formation|36293|2|Defined|p144|Jurassic|Jurassic|||||||
3266|Cadda Formation|36890|3|Fully described|p241|||||||||
3266|Cadda Formation|36911|6|Mentioned|p58|||||||||
3266|Cadda Formation|37104|6|Mentioned|Fig.3|||||||||
3266|Cadda Formation|37308|5|Briefly described|Table 4|||||||||
3266|Cadda Formation|38479|6|Mentioned|p14|||||||||
3266|Cadda Formation|39155|6|Mentioned|Table 2|||||||||
3266|Cadda Formation|39156|6|Mentioned|Table 4|||||||||
3266|Cadda Formation|40300|6|Mentioned|p1|||||||||
3266|Cadda Formation|40992|6|Mentioned|Fig.5|||||||||
3266|Cadda Formation|41172|5|Briefly described|p127|||||||||
3266|Cadda Formation|41195|6|Mentioned|Fig.2|||||||||
3266|Cadda Formation|41284|6|Mentioned|p90|||||||||
3266|Cadda Formation|41681|6|Mentioned|p22|||||||||
3266|Cadda Formation|41728|6|Mentioned|p441|||||||||
3266|Cadda Formation|41729|5|Briefly described|p454|||||||||
3266|Cadda Formation|41989|4|Described|p109|||||||||
3266|Cadda Formation|42075|5|Briefly described|Fig.7 P247|||See also P229||||||
3266|Cadda Formation|42194|6|Mentioned|p18|||||||||
3266|Cadda Formation|43031|4|Described|p20,Fig.2.|||||||||
3266|Cadda Formation|43062|5|Briefly described|Table 2,p18|||||||||
3266|Cadda Formation|43197|5|Briefly described|Map Legend||Jurassic|||||||
3266|Cadda Formation|43216|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
3266|Cadda Formation|43217|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
3266|Cadda Formation|43296|5|Briefly described|Map Legend||Jurassic|||||||
3266|Cadda Formation|43297|3|Fully described|Fig.3p5,p13.|Bajocian|Aalenian|See also Table 1 p6. Type section location given.||||||21-JUL-09
3266|Cadda Formation|43347|4|Described|5|Bajocian|Aalenian|||||||
3266|Cadda Formation|43495|4|Described|3-36|Bajocian|Aalenian|||||||
3266|Cadda Formation|43504|4|Described|4-11|Bathonian|Aalenian|||||||
3266|Cadda Formation|43710|6|Mentioned|p6||Bajocian|||||||
3266|Cadda Formation|43924|14|Not recorded|p14||Bajocian|M.Bajocian age.||||||
3266|Cadda Formation|44144|4|Described|p505 Tb.4-21, p509 Fig.4-145, p514-515|Bathonian|Aalenian|Type Section: Cadda Spring 30o24'20''S 115o16'0''E. 392m thick shallow marine sediments.||||Conformably overlies Cockleshell Gully Formation. Interfingers with lower Yarragadee Formation. Correlates with Champion Bay Group.|Grey shale, siltstone, and sandstone with lenticular carbonate beds.|
3266|Cadda Formation|44237|14|Not recorded|p.201|||||||||
3266|Cadda Formation|44307|14|Not recorded|p11,12,13|||||||||
3266|Cadda Formation|48614|14|Not recorded|p1-5,24 Pl,1,2,9|||(H50-5,9).||||||
3266|Cadda Formation|48848|14|Not recorded|p.99,100|||||||||
3266|Cadda Formation|49942|5|Briefly described|p39|Jurassic|Jurassic|Geological Province: Perth Basin. Possibly an oil source rock.||||||
3266|Cadda Formation|50085|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Northern Perth Basin.||||||11-MAY-04
3266|Cadda Formation|50107|5|Briefly described|Map legend|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
3266|Cadda Formation|60376|4|Described|p16, p29, p17 Fig. 4.|Middle Jurassic|Jurassic|Geological Province: Perth Basin. Overlain by Yarragadee Formation. Underlain by Cattamarra Coal Measures. Consists of shale, siltstone and medium- to very coarse-grained sandstone. Outcrops as Champion Bay Group near Geraldton.||||||07-FEB-11
3266|Cadda Formation|60384|6|Mentioned|p243 Fig 2a, p261|Middle Jurassic|Middle Jurassic|Perth Basin. Source rocks||||||
3266|Cadda Formation|60386|6|Mentioned|p299|Middle Jurassic|Middle Jurassic|Perth Basin. Distal shelf/basin.||||||
3266|Cadda Formation|60997|5|Briefly described|p138|Jurassic|Jurassic|Geological Province: Perth Basin (WA).||||||
3266|Cadda Formation|61023|5|Briefly described|p20 Fig 10|Jurassic|Jurassic|Geological Province: Perth Basin.||||||10-APR-08
3266|Cadda Formation|61546|6|Mentioned|p383 Fig.3, p385 Fig.5. |Jurassic|Jurassic|Has a high amplitude seismic event near the top.||||Overlies Cattamarra Coal Measures Member. Is overlain by Yarragadee Formation.||
3266|Cadda Formation|61811|5|Briefly described|p3 Fig.2, p29, p39, p48, p62.|Middle Jurassic|Middle Jurassic|Northern Perth Basin. Is laterally equivalent to Champion Bay Group, further to the north. A poor but fossiliferous exposure occurs on the west side of Enanty Hill. Type section details in Appendix 1.||||Overlies Cattamarra Coal Measures. Is overlain by Yarragadee Formation.||
3266|Cadda Formation|64580|4|Described|map legend||Middle Jurassic|Grey shale, siltstone and sandstone; scattered carbonate lenses.||||||09-DEC-08
3266|Cadda Formation|64635|5|Briefly described|p4 Fig.3, p16, p23, p28    |Bajocian|Aalenian|Has a poor but fossiliferous exposure on the west side of Enanty Hill.||||Overlies Cattamarra Coal Measures. Upper part is laterally equivalent to the upper Yarragadee Formation.||
3266|Cadda Formation|67135|5|Briefly described|p5 Fig.7.|Jurassic|Jurassic|Perth Basin.||||Overlies Cattamarra Coal Measures. Is overlain by Yarragadee Formation.||
3266|Cadda Formation|67340|6|Mentioned|p6-8, 25, 50-63|Jurassic|Jurassic|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.||||||
3266|Cadda Formation|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Bajocian|Aalenian|||||Overlies the Cattamarra Coal Measures, Cockleshell Gully Formation. Overlain by the Yarragadee Formation.||
3266|Cadda Formation|68135|5|Briefly described|p52 fig 2b |Bathonian|Aaelenian|Perth Basin. Hosts macro-invertebrate fossil assemblages. ||||Overlies Catamarra Member, overlain by Yarragadee Formation|Interbedded siltstone and limestone.|14-SEP-17
3266|Cadda Formation|68254|6|Mentioned|p1036 Fig.2|Jurassic|Jurassic|||||||
3266|Cadda Formation|69081|5|Briefly described|p736,p729,p740,p741, Figs.2-4, Tbs.1-3|Middle Jurassic|Middle Jurassic|Presented as Cadda Fm in Fig.1 and Cadda in other figures and tables. Geol. Prov: Perth Basin||||is overlain by Yarragadee Formation; overlies Cattamarra Coal Measures||
3266|Cadda Formation|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p14|Middle Jurassic|Middle Jurassic|Perth Basin. Forms a regiona seal along with the Eneabba Formation. In excess of 300m. See also Ch2 p20-p29, Ch2 p34-p42, Ch2 p44, Ch2 p46, Ch2 p52-p53, Ch2 p55, Ch2 p57, Ch2 p60-p63, Ch2 p67, Ch2 p74, Ch2 p84-p86, Ch2 p99, Ch2 p100, Ch2 p103-p111.|||||Limestones, marl, shales and claystones.|
3266|Cadda Formation|70097|5|Briefly described|p2, p19-21 Figs.3-5|Bajocian|Bajocian|Transgression in Perth Basin peaked in an extensive but short-lived marine flooding event in the Bajocian. Perth Basin. Beermullah Trough, Mandurah Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies Cattamarra Coal Measures. Is overlain by Yarragadee Formation.|Sedimentary deposition includes sandstone.|12-SEP-17
3266|Cadda Formation|70128|5|Briefly described|p449, p454, p457, p459-462, p464|Middle Jurassic|Middle Jurassic|Northern Perth Basin. Modelled thickness distribution histogram.||||Conformably overlies Cattamarra Coal Measures. Is overlain conformably by Yarragadee Formation.||
3266|Cadda Formation|70826|6|Mentioned|p7 tbl 4|Early Cretaceous|Jurassic|Perth Basin.||||||
3266|Cadda Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||siltstone, biocarboante, sandstone|
3266|Cadda Formation|71377|5|Briefly described|p7|Middle Jurassic|Middle Jurassic|Mandurah Terrace, Perth Basin.||||||
3266|Cadda Formation|71958|5|Briefly described|p34|Bajocian|Aalenian|Vlaming Sub-basin.||||Overlies the Cattamarra Coal Measures. Overlain by the Yarragadee Formation.||
3266|Cadda Formation|72034|5|Briefly described|500k_interpgeop16_lut|Bathonian|Bajocian|Perth Basin.  Age from biostratigraphy.|||||Grey shale, siltstone and sandstone; scattered carbonate lenses.|
3266|Cadda Formation|72258|5|Briefly described|p129|Middle Jurassic|Middle Jurassic|Of Perth Basin.||||Overlain by, and laterally grades southward into Yarragadee Formation. Underlain by Cattamarra Coal Measures.||
3266|Cadda Formation|73513|5|Briefly described|p30 Fig.2|Bajocian|Bajocian|Perth Basin.||||Overlies Cattamarra Coal Measures, underlies Yarragadee Formation|Marine rocks.|
3276|Cadgerina Dyke|42840|5|Briefly described|p290|||||||||
3276|Cadgerina Dyke|43597|6|Mentioned|Fig.1 p717|||||||||
3360|Calooli Monzogranite|42697|5|Briefly described|map legend|Archean||||||||07-NOV-08
3360|Calooli Monzogranite|42698|5|Briefly described|map legend|||||||||
3360|Calooli Monzogranite|42892|4|Described|p43|||||||||
3360|Calooli Monzogranite|43125|5|Briefly described|Fig.3|||||||||03-MAR-10
3360|Calooli Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
3360|Calooli Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmc]   Equigranular, medium- to coarse-grained biotite bearing monzogranite.||||||
3360|Calooli Monzogranite|65204|6|Mentioned|p18 Tbl.3.|Neoarchean||Medium-coarse grains; equigranular.||||||
3360|Calooli Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained, equigranular bitotie monzogranite; generally massive, foliated near margins.||||||07-FEB-11
3360|Calooli Monzogranite|65834|6|Mentioned|p21, 49-50|||Coolgardie Domain, Kalgoorlie Terrane.||Bali Suite.||||
3360|Calooli Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained, equigranular biotite monzogranite; generally massive, foliated near margins.|05-AUG-15
3360|Calooli Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Medium- to coarse-grained, equigranular biotite monzogranite; minor granodiorite and tonalite; metamorphosed.|
3360|Calooli Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
3360|Calooli Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Monzogranite; minor granodiorite and tonalite; metamorphosed|
3360|Calooli Monzogranite|73391|6|Mentioned|p300|||Kalgoorlie district.||||||
3364|Calwynyardah lamproite|41158|6|Mentioned|p157|||||||||
3470|Canning Basin Limestone|24424|5|Briefly described|p539 Tb.4|Late Devonian|Late Devonian|Age: 354-369 Ma. Palaeomagnetic poles given.||||||
3470|Canning Basin Limestone|42141|6|Mentioned|Fig.3 P570|||||||||
3482|Cap Shale|32189|6|Mentioned|Fig.1|||||||||
3509|Cape Londonderry Formation|13194|4|Described|p386 Tb. 4-16, p396 fig 4-60|Middle Triassic|Early Triassic|Type Section: Petrel 1 well (2471-2887m). 280-450m thick continental deposits.||Troughton Group||Overlies Mount Goodwin Formation (conformably). Laterally equivalent to Sahul Group. Overlain by Malita Formation.|Sandstone; minor siltstone and shale.|
3509|Cape Londonderry Formation|13222|5|Briefly described|p229 Fig.2.|Middle Triassic|Middle Triassic|||Unit in Troughton Group.|||Sandstones.|
3509|Cape Londonderry Formation|13234|6|Mentioned|p250 Fig.2,|Triassic|Triassic|||||Overlies Mount Goodwin Formation, offshore.||
3509|Cape Londonderry Formation|13242|5|Briefly described|p225|||Unconformably overlies Upper Mount Goodwin Formation in the Timor Sea. Includes sandstones.||||||07-FEB-11
3509|Cape Londonderry Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Triassic|||||||01-MAR-10
3509|Cape Londonderry Formation|23377|6|Mentioned|p212 Fig.5||Triassic|Of Vulcan Sub-basin.||||||03-AUG-06
3509|Cape Londonderry Formation|24569|5|Briefly described|p248 Fig. 3|Anisian|Scythian|Of the Troughton Group. Geological Province: Petrel Sub-basin.||||||17-MAR-05
3509|Cape Londonderry Formation|41459|6|Mentioned|Fig.2|||||||||
3509|Cape Londonderry Formation|41532|3|Fully described|p304|||||||||
3509|Cape Londonderry Formation|41731|6|Mentioned|Fig.3|||||||||
3509|Cape Londonderry Formation|42055|4|Described|Fig.1 P52|||||||||
3509|Cape Londonderry Formation|42056|5|Briefly described|p98|||||||||03-AUG-06
3509|Cape Londonderry Formation|42442|3|Fully described|p23|Ladinian|Early Triassic|Age: Early Triassic (Smithian to Ladinian)||||||
3509|Cape Londonderry Formation|43661|6|Mentioned|Fig.3|||||||||
3509|Cape Londonderry Formation|43699|6|Mentioned|Fig.6,p10|Late Triassic|Middle Triassic|||||||
3509|Cape Londonderry Formation|43739|6|Mentioned|Fig.5,p38||Triassic|||||||
3509|Cape Londonderry Formation|49637|5|Briefly described|p7|Middle Triassic|Middle Triassic|Fluviodeltaic sediments - mixed clastic-carbonate sequence with minor coals and volcanics. Overlies Mount Goodwin Formation. Geological Province: Petrel Sub-basin.See also Fig. 3||||||07-FEB-11
3509|Cape Londonderry Formation|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Middle Triassic|Of the Troughton Group. Age: ~240-235Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
3509|Cape Londonderry Formation|63929|6|Mentioned|p131 Fig.2.|Middle Triassic|Middle Triassic|Petrel Sub-basin.||||Overlies Mount Goodwin Formation.||
3509|Cape Londonderry Formation|64690|5|Briefly described|p504 Fig.2 |Middle Triassic|Early Triassic|||||Overlies Upper Mount Goodwin Formation.||
3509|Cape Londonderry Formation|64692|6|Mentioned|p522 Fig.2 |Middle Triassic|Early Triassic|Bonaparte Basin.||||Overlies Upper Mount Goodwin Formation.||
3509|Cape Londonderry Formation|66124|5|Briefly described|p171 Fig.2|Anisian|Ladinian|Petrel Sub-basin. Non-marine. Overlies Mount Goodwin Formation.||||||
3509|Cape Londonderry Formation|67370|6|Mentioned|p313 Fig.2, p314 Fig.3, p323 Fig.14.  |Triassic|Triassic|Bonaparte Basin. Type section is in Petrel-1 between 2,471 - 2,887 m.||Unit in Troughton Group.||Overlies Osprey Formation. Is overlain by Malita Formation.||
3509|Cape Londonderry Formation|69452|5|Briefly described|p36:8, 15, 21|Late Triassic|Middle Triassic|Petrel Sub-basin, Bonaparte Basin. Up to 400m thick. The lower and upper parts of the Formation are respectively equivalent to the Osprey and Pollard Formations elsewhere in the Basin.||Troughton Group.||Lower part is equivalent to Osprey Formation.|A regressive succession of sandstone and minor siltstone and shale.|12-JUL-16
3509|Cape Londonderry Formation|69454|5|Briefly described|p38:4|Norian|Anisian|Petrel Sub-basin, Bonaparte Basin.||Troughton Group.||||12-JUL-16
3509|Cape Londonderry Formation|69456|6|Mentioned|p40:3|||Bonaparte Basin.||Troughton Group.||||12-JUL-16
3509|Cape Londonderry Formation|69653|6|Mentioned|p10|Late Triassic|Middle Triassic|Petrel Sub-basin. Presented as Cape Londonberry Formation.||Troughton Group.||Overlies Fishburn Formation (Kinmore Group). Is overlain by Malita Formation.||
3509|Cape Londonderry Formation|69673|5|Briefly described|p153 fig 125, p173|||||Troughton Group||Overlain by Malita Formation, overlies Fishburn Formation|Sandstone, siltstone and shale.|
3509|Cape Londonderry Formation|69689|6|Mentioned|p16|Triassic|Triassic|Bonaparte Basin.||||||
3509|Cape Londonderry Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3|Norian|Middle Triassic|See also Regional geology: Figs.6-7, p5. Part of a succession (with Quoin Formation) of NW-thickening, shallow marine to fluvio-deltaic Permian and Triassic sediments across the Bonaparte Basin. The lower part of this unit is equivalent to the Osprey Formation.||Troughton Group.||Is overlain by Malita Formation.||12-JUL-16
3512|Cape Naturaliste gneiss|37468|6|Mentioned|Table II|||||||||
3521|Cape Range Group|13615|6|Mentioned|p101|Late Miocene|Middle Miocene|Peedmullah Shelf stratigraphy: thickness 20-30 m. Type section Mount Lefroy 23deg13'S, 114deg0'20"E. Rich corals, algae, foraminifera, shells. Middle to innershelf, moderate to high energy, minor lagoonal.|||Includes the Trealla Limestone.|Unconformable on Cardabia Group and older rocks.|Commonly pure calcirudite, calcarenite, calcisiltite.|07-FEB-19
3521|Cape Range Group|14228|6|Mentioned|p9|Miocene|Miocene||||Trealla Limestone.|||
3521|Cape Range Group|22814|5|Briefly described|fig2|Cenozoic|Cenozoic|||||||19-NOV-08
3521|Cape Range Group|23726|5|Briefly described|p88|Middle Miocene|Late Oligocene|Max. thickness: >1000 m.||||||
3521|Cape Range Group|23815|5|Briefly described|p302|||Geological Province: Carnarvon Basin. Contains the Mandu Calcarenite and Tulki Limestone.||||||
3521|Cape Range Group|24059|5|Briefly described|p132|Tertiary|Tertiary|Geological Province: Barrow Sub-basin.||||||
3521|Cape Range Group|24160|6|Mentioned|p37 Fig.12|Tertiary|Tertiary||||||Limestone.|
3521|Cape Range Group|24331|5|Briefly described|p475 Fig.2|Miocene|Miocene|Unconformably overlies Giralia Calcarenite. Marine. Geological Province: Barrow Sub-basin.||||||
3521|Cape Range Group|24541|6|Mentioned|p61|||||||||
3521|Cape Range Group|24543|5|Briefly described|Map legend|Miocene|Miocene|||||||
3521|Cape Range Group|30122|6|Mentioned|p50|||||||||
3521|Cape Range Group|30304|5|Briefly described|p53|||Tertiary age.||||||11-APR-08
3521|Cape Range Group|30875|6|Mentioned|p10|||Lower Miocene age. See also p13.||||||12-SEP-18
3521|Cape Range Group|31561|6|Mentioned|p302|||Refers Chapman (1927)||||||
3521|Cape Range Group|32166|6|Mentioned|p159|||||||||
3521|Cape Range Group|32648|6|Mentioned|p32|||Tertiary||||||
3521|Cape Range Group|32750|6|Mentioned|p302|||Refers Chapman (1927)||||||
3521|Cape Range Group|32752|6|Mentioned|p337|||||||||
3521|Cape Range Group|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
3521|Cape Range Group|33386|6|Mentioned|Fig.7|||||||||
3521|Cape Range Group|33453|6|Mentioned|p72|||Stratigraphy.||||||
3521|Cape Range Group|34363|6|Mentioned|p56|||Lower Miocene. See Fig.7.||||||
3521|Cape Range Group|34846|6|Mentioned|Fig.3|||||||||
3521|Cape Range Group|35059|6|Mentioned|p205|||||||||
3521|Cape Range Group|35105|6|Mentioned|Fig.58|||||||||
3521|Cape Range Group|35282|6|Mentioned|Fig.21|||||||||
3521|Cape Range Group|36257|6|Mentioned|Table 2.1|||||||||
3521|Cape Range Group|36890|3|Fully described|p302|||||||||
3521|Cape Range Group|37016|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
3521|Cape Range Group|37320|6|Mentioned|p237|||||||||
3521|Cape Range Group|38485|5|Briefly described|p17|||||||||
3521|Cape Range Group|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
3521|Cape Range Group|39427|6|Mentioned|p13|||||||||
3521|Cape Range Group|39486|6|Mentioned|Fig.2|||||||||
3521|Cape Range Group|40992|6|Mentioned|Fig.8|||||||||
3521|Cape Range Group|41271|3|Fully described|p175|||||||||
3521|Cape Range Group|41436|6|Mentioned|Fig.6|||||||||
3521|Cape Range Group|41438|5|Briefly described|p111|||||||||
3521|Cape Range Group|41439|6|Mentioned|Fig.4|||||||||
3521|Cape Range Group|41440|6|Mentioned|p139|||||||||
3521|Cape Range Group|41443|6|Mentioned|Fig.3|||||||||
3521|Cape Range Group|41444|6|Mentioned|Fig.4|||||||||
3521|Cape Range Group|41732|6|Mentioned|Fig.3|||||||||
3521|Cape Range Group|42116|5|Briefly described|p69|||||||||
3521|Cape Range Group|43712|6|Mentioned|Fig.10,p52|Miocene|Oligocene|||||||
3521|Cape Range Group|43724|6|Mentioned|Fig.15,p65|Miocene|Oligocene|||||||
3521|Cape Range Group|44159|5|Briefly described|Table p.37||Early Miocene|||||||
3521|Cape Range Group|44959|4|Described|p.21||Miocene|||||||
3521|Cape Range Group|45015|5|Briefly described|map legend|Tertiary|Tertiary|Consists of Trealla Limestone, Tulki Limestione, & Mandu Calcarenite. Age is Late Tertiary.||||||01-JUN-06
3521|Cape Range Group|45142|6|Mentioned|p25|||See also Fig.4.||||||
3521|Cape Range Group|46950|6|Mentioned|Fig.15|||||||||
3521|Cape Range Group|46983|6|Mentioned|Fig.2|||||||||
3521|Cape Range Group|49942|5|Briefly described|p11|Cenozoic|Cenozoic|Geological Province: Gascoyne Platform.||||||19-NOV-08
3521|Cape Range Group|50085|5|Briefly described|p23 Fig. 12|Neogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
3521|Cape Range Group|61023|5|Briefly described|p27 Fig. 12|Neogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
3521|Cape Range Group|61155|5|Briefly described|p15|Late Miocene|Early Oligocene|Includes Mandu, Bullara, Tulki, and Trealla Limestones, Lamont, Bare, and Vlaming Sandstone, Pilgramunna and Pindilya Formation.  Age: 32 - ~6Ma. Geological Province: Carnarvon Basin.||||||03-MAR-10
3521|Cape Range Group|61958|5|Briefly described|Map sheet 1|Neogene|Neogene|Includes: Mandu Calarenite, Tulki Limestone and Trealla Limestone.||||||21-MAR-06
3521|Cape Range Group|62837|5|Briefly described|Stratigraphic columns|Middle Miocene|Oligocene|Age: 25-~16Ma. Geological Province: Dampier Sub-basin, Rankin Platform and Beagle Sub-basin.||||||01-MAR-10
3521|Cape Range Group|63950|5|Briefly described|p336 Fig. 4|Miocene|Oligocene|Geological Province: northern Carnarvon Basin.||||||01-FEB-10
3521|Cape Range Group|64977|6|Mentioned|p493 Fig.3.|Neogene|Neogene|Thevenard Island area.||||Unconformably overlies Giralia Calcarenite.||
3521|Cape Range Group|66125|6|Mentioned|p132||||||||A warm water association of lepidocyclinid-dominated grainstones, packstones and bioturbated wackestones.|
3521|Cape Range Group|67200|6|Mentioned|p17 table 1, p53|||Thermal conductivity of 1.68 W/mK||||||
3521|Cape Range Group|67970|5|Briefly described|p25 Fig.4.|Tortonian|Rupelian|Exmouth Plateau.|||Includes Mandu Formation and Trealla Limestone.|||
3521|Cape Range Group|68811|5|Briefly described|p107, 108, p130, p156 app 1, p191 tbl 45|Tertiary|Tertiary|Inplied to include Mandu Limestone, Tulki Limestone, Trealla Limestone.||||Overlies the Birdrong Sandstone.|Friable to dense fossiliferous limestone and marl with local interbeds of sand.|16-APR-20
3521|Cape Range Group|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|||Carnarvon Basin. See also Ch3 p17-p20, Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p65-p66, Ch3 p73.|||Includes the Trealla Limestone.|Overlies the Gearle Siltstone.||
3521|Cape Range Group|69692|6|Mentioned|p4|Miocene|Oligocene|Northern Carnarvon Basin.||||Overlies Walcott Formation. Is overlain by Delambre Formation.||
3521|Cape Range Group|70066|5|Briefly described|Dampier: Fig.2. Exmouth: Fig.2|Miocene|Oligocene|See also Regional: Fig.6. Northern Carnarvon Basin.|||Mandu and Trealla Limestones; Bare Formation.|Overlies Giralia Calcarenite and Walcott Formation. Is overlain by Delambre Formation.||
3521|Cape Range Group|70826|6|Mentioned|p7 tbl 4|Miocene|Oligocene|Northern Carnarvon Basin.||||||
3521|Cape Range Group|70906|5|Briefly described|p758|Miocene|Miocene|Gorgon Platform.||||Overlies Walcott Formation. Is overlain by Delambre Formation.||
3521|Cape Range Group|72034|5|Briefly described|500k_interpgeop16_lut|Miocene|Oligocene|Northern Carnarvon Basin.  Age from biostratigraphy.|||||Undivided coralgal boundstone, packstone and wackestone, calcarenite, calcareous sandstone.|
3558|Capricorn Group|24544|4|Described|p45|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Upper Wyloo Formation. Unconformably overlain by Mount Minnie Group. Fluvial to shallow marine sandstones, siltstones, minor conglomerate and dolomite. Max thickness: 800m. Supersedes Capricorn Fm. Geol. Prov: Ashbuton Province.||||||07-NOV-08
3558|Capricorn Group|24607|5|Briefly described|p969|Paleoproterozoic|Paleoproterozoic|Age: 1804 +/- 7 Ma from Koonong Member tuff. Max. Thickness: 800m. Geological Province: Blair Basin.||||Unconformably overlies Ashburton Formation||30-NOV-10
3558|Capricorn Group|50216|5|Briefly described|p209|Paleoproterozoic|Paleoproterozoic|Geological Province: Blair Basin.||||||07-NOV-08
3558|Capricorn Group|50225|5|Briefly described|p386 Fig. 1, p388|Paleoproterozoic|Paleoproterozoic|Age: c.1805Ma (Hall et al, 2001).||||||07-FEB-11
3558|Capricorn Group|60301|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Age: c. 1804Ma. Geological Province: Blair Basin. Includes: Bywash Formation.||||||
3558|Capricorn Group|61262|6|Mentioned|p446 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: >1780Ma.  In the Ashburton Basin.||||||07-NOV-08
3558|Capricorn Group|63866|5|Briefly described|p151, p154, p162|||Ashburton Basin.|1804 +/- 7 Ma (Hall et al., 2001)||Includes the Bywash Formation, Mooline Formation.|Overlies the Wyloo Group. Unconformably overlain by the Edmund Group.||
3558|Capricorn Group|63869|4|Described|p1, p4-5, p6, p7-9, p14, p15, p28|Paleoproterozoic|Paleoproterozoic|See also p47, p49, p51, p55, Plate 1. Blair Basin. Rocks formerly assigned to Wyloo Group (Horwitz, 1980; Seymour et al., 1988); subsequently assigned to Capricorn Formation (Thorne and Seymour, 1991) due to an unconformity; later raised to Group level (this study) due to recognition of two lithostratigraphic units. Type section is the same as that proposed by Thorne and Seymour (1991) for the Formation; details given. Strongly diachronous sedimentation, 1.5 - 3 km thick. SHRIMP U-Pb zircon age from a felsic volcanic unit.|1804 +/- 7 Ma (Hall et al., 2001).||Includes Bywash and Mooline Formations.|Unconformably overlies Wyloo Group. Is overlain unconformably by Edmund Group.|Metasedimentary and metavolcanic rocks; sandstone, siltstone and mudstone, and small amounts of conglomerate, dolostone and felsic volcanic rock.|
3558|Capricorn Group|64580|4|Described|map legend||Paleoproterozoic|Conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock.||||||09-DEC-08
3558|Capricorn Group|64724|6|Mentioned|p45 Fig.5|Orosirian|Orosirian|Ashburton Basin.||||||
3558|Capricorn Group|64728|6|Mentioned|p94 Fig.1, p95, p106.|||Low-grade metasedimentary rocks.|Depositional age is c.1800 Ma.|||Unconformably overlain by Bangemall Supergroup.||
3558|Capricorn Group|65506|6|Mentioned|p987 Fig.1A|||||||||
3558|Capricorn Group|65830|5|Briefly described|p3, p4, p13; Plates 1,2|Orosirian|Orosirian|Previously the Capricorn Formation. Blair Basin.|~1804 +/- 7 Ma.||Includes Bywash Formation, Mooline Formation.|Underlain by the Wyloo Group. Unconformably underlain by the Ashburton Formation.||
3558|Capricorn Group|66299|5|Briefly described|p202.|Paleoproterozoic|Paleoproterozoic|Ashburton Fold Belt.|c.1790 Ma.||Includes Bywash Formation.|Unconformably overlies Ashburton Formation.||
3558|Capricorn Group|66950|6|Mentioned|p18|||||||Unconformably overlies the Ashburton Formation.||15-DEC-16
3558|Capricorn Group|68981|5|Briefly described|p3 Fig.1, p20, p22|||Thorne and Seymour (1991). Blair Basin. Deposition associated with the 1820-1770 Ma Capricorn Orogeny. Terrestrial, lacustrine to shallow-marine sedimentary rocks. Sediments supplied from the SW.|c.1800 Ma (Hall et al., 2001).|||Unconformably overlies the Wyloo Group.||
3558|Capricorn Group|69003|5|Briefly described|p4, p24-26, p36|||Blair Basin, Capricorn Orogen. c.2km thick. Deposition was broadly synchronous with the Yapungku Orogeny. Most sediments were sourced from the Glenburgh Terrane.|c.1786 Ma.|||Is overlain unconformably by Edmund Group.|Fluvial to shallow-marine sandstones.|
3558|Capricorn Group|69024|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Blair Basin. See map legend for a detailed lithological description.|||Includes the Mooline Formation and Bywash Formation.||Includes sandstone, siltstone, conglomerate, dolostone, dolomitic siltstone, felsic volcaniclastic sandstone, dololutite, dolorudite, and felsic volcanic rock.|
3558|Capricorn Group|69028|5|Briefly described|Map Legend|Orosirian|Orosirian|Ashburton and Blair Basins. These two Formations are mapped as a single unit.|c.1805 Ma.||Includes the Bywash Formation and the Mooline Formation.||Includes conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock.|07-MAY-14
3558|Capricorn Group|69080|4|Described|p684, p687-689|Statherian|Orosirian|Blair Basin, Pilbara Craton. Deposited after the early deformation stage of the 1820-1770 Ma Capricorn Orogeny; possibly strongly diachronous.|c.1804 Ma (Hall et al., 2001).|||Unconformably overlies Ashburton Formation (Wyloo Group).|Conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone and felsic volcanic rock.|
3558|Capricorn Group|69166|6|Mentioned|geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic||||Includes Bywash Formaiton, Mooline Formation|||
3558|Capricorn Group|69185|4|Described|500k_geologyp08_lut.csv||Paleoproterozoic|Geological Province: Pilbara Craton.|||||Undivided; conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock|
3558|Capricorn Group|69387|5|Briefly described|p3, p7|||Ashburton Basin.|1830-1800 Ma.|||||13-JUN-17
3558|Capricorn Group|69596|5|Briefly described|p4-5, p8 Fig.5|Paleoproterozoic|Paleoproterozoic|Blair Basin, Capricorn Orogen.|c.1804 Ma.||||Siliciclastic sedimentary rocks.|
3558|Capricorn Group|70795|6|Mentioned|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 2_5m_interpgeop15_lut.csv, 148922.1.pdf|1801-1738 Ma||Includes Mooline Formation, Bywash Formation||Ferruginous lithic and dolomitic quartz sandstone, ferruginous siltstone and mudstone, conglomerate, dolostone and felsic volcanic rock.|
3558|Capricorn Group|70814|5|Briefly described|p3, p8, p32, p34, p35 fig 19, p41, p73|Paleoproterozoic|Paleoproterozoic||1805-1783 Ma||Includes the Mooline Formation.|Unconformably overlain by the Yilgatherra Formation and the Irregully Formation.||
3558|Capricorn Group|70826|6|Mentioned|p6 tbl 2, p10|Paleoproterozoic|Paleoproterozoic|Blair Basin.||||||21-APR-20
3558|Capricorn Group|70949|6|Mentioned|p988|Mesoproterozoic|Mesoproterozoic|||||||
3558|Capricorn Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, conglomerate, sandstone|
3558|Capricorn Group|71795|6|Mentioned|p32 fig 1|||||||||
3558|Capricorn Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Blair Basin.|Max age 1804+/-7 Ma, min ~1738 Ma.||||Ferruginous lithic and dolomitic quartz sandstone, ferruginous siltstone and mudstone, conglomerate, dolostone, and felsic volcanic rock.|
3558|Capricorn Group|72712|6|Mentioned|p2 Fig.1, p3, p49.|Orosirian|Orosirian|Included as part of the definition of the Hamersley province.||||Shown as overlying Shingle Creek Group.||
3558|Capricorn Group|73102|5|Briefly described|p3, p20, p25-26|||Ashburton Basin. Pilbara Craton.||||Intruded by Kulkatharra Dolerite.|Ferruginous lithic and dolomitic quartz sandstone, ferruginous siltstone and mudstone, conglomerate, dolostone, and felsic volcanic rock.|
3558|Capricorn Group|73168|6|Mentioned|p765|Paleoproterozoic|Paleoproterozoic|Blair Basin. Deposited in an extensive foreland basin system accompanying onset of the Capricorn Orogen.|||||Volcano-sedimentary rocks.|
3558|Capricorn Group|73442|5|Briefly described|p3|||Pilbara Craton.|||||Conglomerate, ferruginous and quartzitic sandstone, ferruginous siltstone and mudstone, dolostone, and felsic volcanic rock.|
3580|Carbla Oolite Member|23726|5|Briefly described|p95 Fig 30|Pleistocene|Pleistocene|Of Dampier Limestone.||||||
3580|Carbla Oolite Member|40342|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
3580|Carbla Oolite Member|40343|5|Briefly described|p13|||||||||
3580|Carbla Oolite Member|41271|4|Described|p197|||||||||
3580|Carbla Oolite Member|69558|5|Briefly described|p98, p226|Pleistocene|Pleistocene|Originally the Carbla Oolite of Logan et al (1970b). Renamed the Carbla Oolite Member by Van de Graaff et al (1983). Deposited during the last interglacial period of the Pleistocene. Exposed at several localities beside the East coast of Hamelin Pool. Forms a hard substrate on which the stromatolites of Shark Bay grow.||Dampier Limestone||||
3589|Cardabia Calcarenite|12471|6|Mentioned|p475 Fig.2.|Paleogene|Paleogene|||||Overlies Toolonga Calcilutite. Is overlain by Trealla Limestone. ?||24-OCT-14
3589|Cardabia Calcarenite|12729|6|Mentioned|p9 Fig.6, p17.|Paleocene|Paleocene|Shallow-marine (Hocking et al., 1987).|||||Limestone.|
3589|Cardabia Calcarenite|13615|4|Described|p101 App.3, p119 App.5|Eocene|Palaeocene|Variation on Cardabia Group also used in this paper. <100m thick. The type section occurs in the Giralia Anticline; 22deg49'20" S 114deg08'00"E. Deposited in a shallow marine, inner shelf setting.||||Disconformably overlies the Toolonga Calcilutite.|Calcarenite and calcisiltite, commonly marly with a basal greensand.|07-FEB-19
3589|Cardabia Calcarenite|14228|5|Briefly described|p5 Fig.2, p9, p16|Eocene|Paleocene|Gascoyne Platform. Up to 77m thick. Does not extend far inland.||||Overlain by Giralia Calcarenite (disconformably).|Flat-lying shallow-marine carbonate strata.|
3589|Cardabia Calcarenite|23403|4|Described|p9|Neogene|Paleogene|Formerly Cardabia Group.||||||24-NOV-09
3589|Cardabia Calcarenite|23572|5|Briefly described|p8 Fig. 6|Paleocene|Paleocene|Geological Province: Carnarvon Basin.||||||
3589|Cardabia Calcarenite|23620|5|Briefly described|p4 Fig. 4|Paleogene|Paleogene|||||||07-NOV-08
3589|Cardabia Calcarenite|23726|5|Briefly described|p8 Fig 2c|Eocene||Overlain by Robe Pisolite. Underlain by Lambert Formation. Geological Province: Carnarvon Basin.||||||05-MAY-08
3589|Cardabia Calcarenite|23915|5|Briefly described|p519 Fig. 2|Paleogene|Paleogene|||||||07-NOV-08
3589|Cardabia Calcarenite|23935|5|Briefly described|p11 Fig.7|Paleocene|Paleocene|Geological Province: Southern Carnarvon Basin.||||||
3589|Cardabia Calcarenite|23976|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
3589|Cardabia Calcarenite|23977|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
3589|Cardabia Calcarenite|23978|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
3589|Cardabia Calcarenite|24331|5|Briefly described|p475 Fig.2|Paleocene|Paleocene|Unconformably overlies Toolonga Calcilutite. Unconformably overlain by Giralia Calcarenite. Marine. Geological Province: Barrow Sub-basin.||||||
3589|Cardabia Calcarenite|24351|5|Briefly described|plate 3, Plate 4 (in pocket)|Paleocene|Paleocene|Geological Province: Exmouth Sub-basin. Log Edel-1.||||||13-DEC-07
3589|Cardabia Calcarenite|24455|5|Briefly described|p327|||Geological Province: Carnarvon Basin.  See also p321 Fig. 1.||||||
3589|Cardabia Calcarenite|40617|5|Briefly described|p14|||Mention p16.||||||05-MAY-08
3589|Cardabia Calcarenite|40992|6|Mentioned|Fig.8|||||||||
3589|Cardabia Calcarenite|41271|3|Fully described|p166|||||||||
3589|Cardabia Calcarenite|41438|6|Mentioned|p110|||See also Fig.23||||||
3589|Cardabia Calcarenite|41440|6|Mentioned|p139|||||||||
3589|Cardabia Calcarenite|41729|6|Mentioned|Fig.2|||||||||
3589|Cardabia Calcarenite|42116|5|Briefly described|Fig.1 P6|||||||||
3589|Cardabia Calcarenite|49942|5|Briefly described|p4 Fig.3|Eocene|Paleocene|Unconformably overlies Miria Marl. Geological Province: Gascoyne Platform.||||||05-MAY-08
3589|Cardabia Calcarenite|50085|5|Briefly described|p23 Fig. 12|Paleogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
3589|Cardabia Calcarenite|60384|6|Mentioned|p244, p243 Fig 2a|Eocene|Paleocene|Carnarvon Basin.||||||
3589|Cardabia Calcarenite|61023|5|Briefly described|p27 Fig. 12|Paleogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
3589|Cardabia Calcarenite|61155|5|Briefly described|p15|Late Paleocene|Late Paleocene|Age: 61.5-49.5Ma. Includes Boongerooda Greensand, Wadera, Pirie, Cashin and Jubilee Members. Geological province: Carnarvon Basin (onshore).||||||03-MAR-10
3589|Cardabia Calcarenite|62837|5|Briefly described|Stratigraphic columns|Paleocene|Paleocene|Age: ~60-55Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
3589|Cardabia Calcarenite|64977|6|Mentioned|p493 Fig.3.|Paleogene|Paleogene|Thevenard Island area.||||Unconformably overlies Toolonga Calcilutite. Is unconformably overlain by Giralia Calcarenite.||
3589|Cardabia Calcarenite|66125|5|Briefly described|p132|||Giralia Anticline.|||||Mixed glauconitic/phosphatic sands interbedded with chalky skeletal packstones/wackestones in which bryozoans, echinoids and foraminifers are common.|
3589|Cardabia Calcarenite|67200|5|Briefly described|p8 fig 6, |Pliocene|Eocene|||||Overlies Lambert Formation,|Limestone and sandstone.|
3589|Cardabia Calcarenite|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|Early Eocene|Paleocene|Carnarvon Basin. Maximum thickness of 77m. See also Ch3 p19-p20, Ch3 p23-p26, Ch3 p35, Ch3 p37, Ch3 p65-p66, Ch3 p69, Ch3 p73. ||||Disconformably overlies the Miria Formation and Toolonga Calcilutite. Disconformably overlain by the Giralia Calcarenite.||
3589|Cardabia Calcarenite|69297|5|Briefly described|p247, p249|Cenozoic|Cenozoic|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Unconformably overlies the Miria Formation. Unconformably overlain by the Trealla Limestone.|Calcarenite.|
3589|Cardabia Calcarenite|70066|5|Briefly described|Regional: Fig.6|Lutetian|Selandian|Exmouth and Barrow Sub-basins, Northern Carnarvon Basin.||||Overlies Lambert or Miria Formation. Is overlain by Giralia Calcarenite.||
3589|Cardabia Calcarenite|70826|6|Mentioned|p7 tbl 4|Eocene|Paleocene|Northern Carnarvon Basin.||||||
3589|Cardabia Calcarenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcilutite, greensand, calcarenite|
3589|Cardabia Calcarenite|72034|5|Briefly described|500k_interpgeop16_lut|Eocene|Paleocene|Marine deposits, Northern Carnarvon Basin.  Age from biostratigraphy.|||||Calcarenite and calcisiltite packstone to wackestone; fossiliferous; commonly marly and glauconitic; basal greensand.|
3594|Cardarie Sandstone Member|40347|5|Briefly described|p21|||||||Overlies Mokadine Formation.|Clean orthoquartzite|06-JAN-15
3601|Cardup Group|22716|5|Briefly described|table4, p239|Neoproterozoic|Neoproterozoic|Unconformably overlies Yilgarn Craton. Age: 750 Ma?||||||
3601|Cardup Group|22812|6|Mentioned|p629|Proterozoic|Proterozoic|||||||
3601|Cardup Group|23773|5|Briefly described|p754|||Age: 750-600 Ma. In the Yilgarn Craton.||||||
3601|Cardup Group|23788|5|Briefly described|p13|Proterozoic|Proterozoic|Geological Province: Yilgarn Craton.||||||
3601|Cardup Group|23816|6|Mentioned|p258|Proterozoic|Proterozoic|||||||
3601|Cardup Group|24058|5|Briefly described|p111|Precambrian|Precambrian|Geological Basin: Perth Basin.||||||
3601|Cardup Group|24160|6|Mentioned|p23, p95|Proterozoic|Proterozoic|Important source of clay and shale for the brick industry. Three Formations, not named. c.500 m thick.|||||Weakly metamorphosed shale, sandstone, minor conglomerate. Intruded by dolerite and quartz veins.|
3601|Cardup Group|24410|5|Briefly described|p141 Fig. 82|||Adjacent to the Darling Fault.||||||24-NOV-09
3601|Cardup Group|24526|5|Briefly described|p114, p106 Fig. 7|Neoproterozoic|Neoproterozoic|Comprises folded shale, sandstone and conglomerate.  Age: >800Ma.  See also p112 Fig. 9.||||||
3601|Cardup Group|24542|5|Briefly described|p2 Fig.2, p11|||Shale, sandstone and conglomerate, cut by dolerite dykes.||||||
3601|Cardup Group|29693|6|Mentioned|p47|||||||||
3601|Cardup Group|29845|6|Mentioned|p198|||||||||
3601|Cardup Group|30592|6|Mentioned|Fig.70|||||||||
3601|Cardup Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
3601|Cardup Group|30883|6|Mentioned|Fig.2|||||||||
3601|Cardup Group|30939|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3601|Cardup Group|31562|6|Mentioned|p5|||||||||
3601|Cardup Group|33044|4|Described|p40|||See also map 3. Group formations||||||
3601|Cardup Group|34702|6|Mentioned|p31|||||||||
3601|Cardup Group|35058|6|Mentioned|p64|||||||||
3601|Cardup Group|35282|6|Mentioned|p9|||||||||
3601|Cardup Group|35979|6|Mentioned|p124|||||||||
3601|Cardup Group|36293|2|Defined|p71|Neoproterozoic|Neoproterozoic|||||||
3601|Cardup Group|36295|6|Mentioned|Fig.2|||||||||
3601|Cardup Group|36872|3|Fully described|p77|||Formerly Armadale Sh.,Cardup-Armadale Sh.,Cardup Series,Cardup Sh.||||||
3601|Cardup Group|37017|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
3601|Cardup Group|37299|6|Mentioned|Fig.1|||||||||
3601|Cardup Group|37344|6|Mentioned|p74|||||||||
3601|Cardup Group|37460|4|Described|p178|||||||||
3601|Cardup Group|37577|6|Mentioned|p56|||||||||
3601|Cardup Group|38769|6|Mentioned|p79|||||||||
3601|Cardup Group|38988|6|Mentioned|p13|||||||||
3601|Cardup Group|40370|6|Mentioned|p39|||||||||
3601|Cardup Group|41341|6|Mentioned|p8|||||||||
3601|Cardup Group|42687|6|Mentioned|map legend|||||||||
3601|Cardup Group|42688|6|Mentioned|map legend|||||||||
3601|Cardup Group|42890|5|Briefly described|p293|||||||||
3601|Cardup Group|42928|5|Briefly described|p451|||||||||
3601|Cardup Group|43038|5|Briefly described|p9|||||||||
3601|Cardup Group|43096|6|Mentioned|p3|||||||||
3601|Cardup Group|43189|5|Briefly described|Map Legend||Proterozoic|||||||
3601|Cardup Group|43212|4|Described|p4,p5.||Neoproterozoic|Formed between c.750 and 600 Ma.||||||
3601|Cardup Group|44138|6|Mentioned|p264 Fig.3-54, p265, p273|||~500m thick of 3 Formations. Aged 750-600 Ma.|||||Weakly metamorphosed shale, sandstone, and minor conglomerate.|
3601|Cardup Group|44144|6|Mentioned|p495, p522|Proterozoic|Proterozoic|Excluded from Perth Basin in this article; a component of Pinjarra Orogen.||||||
3601|Cardup Group|45965|14|Not recorded|p.58|||||||||
3601|Cardup Group|60556|5|Briefly described|p2 Fig. 2, p3|Proterozoic||||||||
3601|Cardup Group|62381|6|Mentioned|p2 Fig.2.|||||||||
3601|Cardup Group|63866|6|Mentioned|p183|||||||||
3601|Cardup Group|64580|4|Described|map legend||Neoproterozoic|Predominantly white to black shale with bands of conglomerate, quartz sandstone and sandstone.||||||09-DEC-08
3601|Cardup Group|64722|5|Briefly described|Fig. 2 p3-6, p20|Neoproterozoic|Neoproterozoic|Lies immediately east of Darling Fault. Minimum age of 590-560 Ma from intruding dyke (Rb-Sr age). Unconformable on Yilgarn basement.|||||Predominantly siliciclastic strata with some volcanic and volcaniclastic rocks and minor dolomite.|11-APR-12
3601|Cardup Group|65487|6|Mentioned|p2 Fig.1, p57 Fig.28|||||||||
3601|Cardup Group|69003|6|Mentioned|vi, p28, p54, p72|||||||||
3601|Cardup Group|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
3601|Cardup Group|69182|6|Mentioned|Ch2 p3|||Perth Basin. ||||||
3601|Cardup Group|69595|6|Mentioned|p3 fig 1|||||||||
3601|Cardup Group|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Pinjarra Orogen.||||||20-MAY-20
3601|Cardup Group|71146|6|Mentioned|p16 |Precambrian|Precambrian|Pinjarra Orogen.||||||
3601|Cardup Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, quarzite, sandstone, shale|
3601|Cardup Group|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Mesoproterozoic|Cardup Basin.|||||Predominantly white to black shale with bands of conglomerate, quartz sandstone, and sandstone.|
3629|Carlton Group|13194|4|Described|p394 Tb. 4-16, p382 fig 4-59, p382|Early Ordovician|Early Cambrian|0-1200m thick shallow marine to intertidal deposits.|||Tarrara, Skewthorpe Formations; Hart Spring, Pretlove, Clark Sandstones; Pander Greensand.|Overlies Antrim Plateau Volcanics (conformably).|Sandstone, siltstone, dolomite.|
3629|Carlton Group|13234|6|Mentioned|p250 Fig.2,|Ordovician|Cambrian|||||||
3629|Carlton Group|22663|5|Briefly described|W97 8 to 10 fig.3|Ordovician|Cambrian|||||||01-MAR-10
3629|Carlton Group|22814|5|Briefly described|fig2|Ordovician|Cambrian|||||||
3629|Carlton Group|23377|6|Mentioned|p212 Fig.5|Early Ordovician|Middle Cambrian|Of Vulcan Sub-basin.||||||03-AUG-06
3629|Carlton Group|24390|5|Briefly described|p2 Fig. 2||Cambrian|Geological Province: Bonaparte Basin.||||||
3629|Carlton Group|24503|5|Briefly described|Map legend|Ordovician|Middle Cambrian|Shallow marine sandstone, siltstone, shale and stromatolitic dolomite. Geological Province: Bonaparte Basin.||||||10-APR-08
3629|Carlton Group|24569|5|Briefly described|p248 Fig. 3|Early Ordovician|Late Cambrian|Geological Province: Petrel Sub-basin.||||||
3629|Carlton Group|32648|6|Mentioned|p32|||Camb. - Ord.||||||
3629|Carlton Group|36257|6|Mentioned|Table 2.1|||||||||
3629|Carlton Group|40993|6|Mentioned|p4|||Mention Fig.1||||||
3629|Carlton Group|41459|6|Mentioned|Fig.2|||||||||
3629|Carlton Group|41690|5|Briefly described|p3|||See also Fig.2||||||
3629|Carlton Group|41731|6|Mentioned|Fig.3|||||||||
3629|Carlton Group|41864|5|Briefly described|p29|||||||||
3629|Carlton Group|41865|6|Mentioned|Map Legend|Early Ordovician|Middle Cambrian|||||||
3629|Carlton Group|43236|6|Mentioned|p14,Fig.13.|Late Cambrian|Early Cambrian|||||||
3629|Carlton Group|43661|6|Mentioned|Fig.3|||||||||
3629|Carlton Group|44159|5|Briefly described|Table p.38|Early Ordovician|Middle Cambrian|||||||
3629|Carlton Group|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
3629|Carlton Group|49637|5|Briefly described|Fig. 6|Early Ordovician|Early Cambrian|Includes Hart Spring, Skewthorpe and Clarke Formations, Pretlove Sandstone and Pander Greensand. Thickness: 1500m. Geological Province: Bonaparte Basin.||||||07-FEB-11
3629|Carlton Group|50085|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin.||||||
3629|Carlton Group|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin.||||||10-APR-08
3629|Carlton Group|64580|4|Described|map legend|Early Ordovician|Middle Cambrian|Sandstone, siltstone, shale, and stromatolitic dolomite; includes TARRARA and SKEWTHORPE FORMATIONS, HART SPRING, PRETLOVE and CLARK SANDSTONES, and PANDER GREENSAND.||||||09-DEC-08
3629|Carlton Group|65449|6|Mentioned|p34|Early Ordovician|Cambrian|Petrel Sub-basin, Bonaparte Basin.||||||
3629|Carlton Group|69099|4|Described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian||||Includes Tarrara and Skewthorpe Formations, Hart Spring, Pretlove and Clark Sandstones, and Pander Greensand||Sandstone, siltstone, shale, and stromatolitic dolomite.|30-JUL-15
3629|Carlton Group|69165|4|Described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian||||Includes Tarrara Formation, Skewthorpe Formation, Hart Spring Sandstone, Pretlove Sandstone, Clark Sandstone, Pander Greensand||Undivided; sandstone, siltstone, shale and stromatolitic dolomite.|
3629|Carlton Group|69437|5|Briefly described|p22:11|Early Ordovician|Late Cambrian|Carlton Sub-basin, Bonaparte Basin.|||Tarrara, Skewthorpe Formations; Hart Spring, Pretlove, Clark Sandstones; Pander Greensand.|||12-JUL-16
3629|Carlton Group|69448|6|Mentioned|p33:3, 7|||Bonaparte Basin.|||Tarrara, Skewthorpe Formations; Hart Spring Sandstone.|||12-JUL-16
3629|Carlton Group|69452|4|Described|p36:2, 4-6|Early Ordovician|Middle Cambrian|Caye (1968). Carlton Sub-basin, SW Bonaparte Basin. Oldest rocks in the Basin. Over 1200m thick.|||Tarrara, Skewthorpe Formations; Hart Spring, Pretlove, Clark Sandstones; Pander Greensand.|Unconformably overlies Antrim Plateau Volcanics. Is overlain unconformably by Cockatoo Group.|Siliciclastic and carbonate rocks.|12-JUL-16
3629|Carlton Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian||||Includes Tarrara Formation, Skewthorpe Formation, Hart Spring Formation, Pretlove Sandstone, Clark Sandstoneand Pander Greensand.||Undivided;  sandstone, siltstone, shale, and stromatolitic dolomite|
3629|Carlton Group|69673|6|Mentioned|p167, p168 fig 139, p179, p185|Ordovician|Cambrian ||||Includes Tarrara Formation, Hart Spring Sandstone, Skewthorpe Formation, Pretlove Sandstone, Clark Sandstone, Pander Greensand|||
3629|Carlton Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Ordovician|Cambrian||470-509 Ma||||Sandstone, siltstone, shale, and stromatolitic dolomite|
3629|Carlton Group|70826|6|Mentioned|p7 tbl 3|Ordovician|Cambrian|Southern Bonaparte Basin.||||||
3629|Carlton Group|70851|6|Mentioned|p17|||||||||
3629|Carlton Group|71146|5|Briefly described|p6|Ordovician|Cambrian|Bonaparte Basin.|||Includes the Tararra Formation, Hart Springs Sandstone, Skewthorpe Formation, Pretlove Sandstone, Clark Sandstone and Pander Greensand.||Mudstone, carbonate and sandstone.|
3629|Carlton Group|71267|4|Described|GEOL_LUT_CSV files|||Of Carlton Shelf, Southern Bonaparte Basin. Events: Gondwana breakup-northern NW Shelf (320-138 Ma); Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||||conglomerate,  stromatolitic dolostone, limestone, sandstone, greensand|
3629|Carlton Group|72034|5|Briefly described|500k_interpgeop16_lut|Early Ordovician|Series 3|Southern Bonaparte Basin. Age from biostratigraphy.|||||Sandstone, siltstone, shale, and stromatolitic dolomite.|
3647|Carnegie Formation|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
3647|Carnegie Formation|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
3647|Carnegie Formation|24301|5|Briefly described|p16|||Geological Province: Amadeus Basin||||||
3647|Carnegie Formation|31393|6|Mentioned|Pl.25|||||||||
3647|Carnegie Formation|31914|6|Mentioned|p96|||U.Proterozoic||||||
3647|Carnegie Formation|33588|6|Mentioned|p6|||||||||
3647|Carnegie Formation|34186|6|Mentioned|Fig.3|||See also Fig.4. Late Precambrian.||||||
3647|Carnegie Formation|35102|6|Mentioned|Fig.2|||||||||
3647|Carnegie Formation|35863|6|Mentioned|Table 1|||||||||
3647|Carnegie Formation|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3647|Carnegie Formation|36551|6|Mentioned|Table 13|||||||||
3647|Carnegie Formation|36887|6|Mentioned|p211|||||||||
3647|Carnegie Formation|37928|6|Mentioned|p517|||||||||
3647|Carnegie Formation|39210|6|Mentioned|Fig.10|||||||||
3647|Carnegie Formation|40740|6|Mentioned|p1|||||||||
3647|Carnegie Formation|41039|6|Mentioned|Fig.2|||||||||
3647|Carnegie Formation|41115|6|Mentioned|Fig.2|||||||||
3647|Carnegie Formation|41852|6|Mentioned|p209|||||||||
3647|Carnegie Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, shale, conglomerate.  Geological province: Amadeus Basin.||||||23-JAN-08
3647|Carnegie Formation|43503|6|Mentioned|50||Proterozoic|||||||
3647|Carnegie Formation|44395|14|Not recorded|p.6,8,12, Tb.1||Proterozoic|(Proterozoic).||||||
3647|Carnegie Formation|44396|5|Briefly described|map legend|||(Proterozoic). SF/52-15.||||||
3647|Carnegie Formation|44439|2|Defined|p.6-9, Tb.1, map||Neoproterozoic|Upper Proterozoic. (G52-2)||||||
3647|Carnegie Formation|44440|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
3647|Carnegie Formation|44499|14|Not recorded|opp.p.6, Tb.1||Proterozoic|||||||
3647|Carnegie Formation|44500|5|Briefly described|map legend||Proterozoic|||||||
3647|Carnegie Formation|45041|4|Described|p30|||Fig.7. Equiv. Areyonga Fm.||||||
3647|Carnegie Formation|45149|6|Mentioned|Table 1|||Page 17.||||||
3647|Carnegie Formation|48842|2|Defined|p.15||Neoproterozoic|p.8,12,15,16-7,20,233,27,30,Pls.5,7,8,Tb.I. (new name). Lat.equiv.to Boord Fm. correlates with Areyonga Fm. Overlies Bitter Springs Limestone; underlies Ellis Sandstone and Sir Frederick Conglomerate. (F52-14,G52-2).||||||05-DEC-06
3647|Carnegie Formation|48862|2|Defined|p.8||Neoproterozoic|On many pages. p.1,8,13-14,30,32,34,38,41; opp.8; Pl.11. U.Proterozoic-?Cambrian.||||||16-JUL-13
3647|Carnegie Formation|48864|14|Not recorded|p.10,78,Pl.10||Neoproterozoic|U.Prot.Defn. on Tech.File G/52-2.||||||
3647|Carnegie Formation|48963|6|Mentioned|Fig.2|||||||||
3647|Carnegie Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, pebbly sandstone and conglomerate.  Geological Province: Amadeus Basin.||||||
3647|Carnegie Formation|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, pebbly sandstone, conglomerate. Geological Province: Amadeus Basin.||||||16-JUL-13
3647|Carnegie Formation|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, pebbly sandstone and conglomerate. Geological Province: Amadeus Basin.||||||14-FEB-06
3647|Carnegie Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
3647|Carnegie Formation|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
3647|Carnegie Formation|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale, conglomerate. Underlies: Ellis Sandstone and Sir Frederick Conglomerate. Overlies: Boord Formation and Bitter Springs Formation.||||||14-AUG-06
3647|Carnegie Formation|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale, conglomerate.||||||
3647|Carnegie Formation|64580|4|Described|map legend||Neoproterozoic|Siltstone, dolomite, diamictite, sandstone, and conglomerate.||||||09-DEC-08
3647|Carnegie Formation|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
3647|Carnegie Formation|65102|6|Mentioned|p363, Figure 4-38, p364|Neoproterozoic|Neoproterozoic|Amadeus Basin. Glacial deposits considered coeval with Savory Group and possibly Yeneena Group.||||||
3647|Carnegie Formation|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
3647|Carnegie Formation|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Overlies Boord Formation conformably and Bitter Springs Formation unconformably.||
3647|Carnegie Formation|67856|4|Described|p341, p338, 337, 339, 344, 345 |Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. Type area: Carnegie Range. Delta or beach red beds. ~1200m thick. Correlation with Areyonga Formation, Inindia beds suggested.||||Conform. overlain by Ellis Sandstone, Sir Frederick Conglomerate. Interfingers w Boord Formation; equiv. to Olympic Formation, Pioneer Sandstone.  Disconformably overlies Bitter Springs Formation.|Silty quartz arenite, sandstone, siltstone, shale, heavy mineral concentrations.|
3647|Carnegie Formation|68270|4|Described|p679,683|Cryogenian|Cryogenian|Amadeus Basin.||||Interfingers westward with Boord Formation.||
3647|Carnegie Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
3647|Carnegie Formation|69003|6|Mentioned|p5, p60|Cambrian|Ediacaran|West Arunta Orogen and western Amadeus Basin.||||||
3647|Carnegie Formation|69031|5|Briefly described|p4, p9|||Amadeus Basin. Formerly thought (Haines et al., 2010) to interfinger with the top of the (then) Boord Formation (now Julie Formation). Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Julie Formation; also Bitter Springs Formation unconformably. Is overlain by Sir Frederick Conglomerate and Ellis Sandstone.|Thick, immature, siliciclastic unit.|
3647|Carnegie Formation|69437|6|Mentioned|p22:8|||Western Amadeus Basin.||||Equivalent (probably) to Arumbera Sandstone.||12-JUL-16
3647|Carnegie Formation|69438|4|Described|p23:2, 4, 10, 17-18, 21, 23, 26|Ediacaran|Ediacaran|Wells et al. (1964). Amadeus Basin. Average thickness (in WA) about 1700m. Overlies Bitter Springs Formation disconformably. Has an upper faulted contact with Mereenie Sandstone. Was previously correlated with Areyonga Formation and Inindia beds, and/or Pertatataka Formation; the stratigraphic succession has been revised.||Pertaoorrta Group.||Overlies (?conformably) Inindia beds. Is correlated with Arumbera Sandstone and Winnall beds. Is overlain by Ellis and Cleland Sandstones conformably and, in WA, Sir Frederick Conglomerate.|Red-brown sandstone, siltstone, minor shale, pebbly sandstone, and conglomerate locally dominated by clasts of dolostone probably derived from the Bitter Springs Formation.|12-JUL-16
3647|Carnegie Formation|69606|4|Described|p1, p3, p4 fig 2, p6 fig 3, p7 fig 4|Lower Cambrian|Upper Ediacaran|western Amadeus Basin. Deposited synchronously with the Petermann Orogeny. >70m thick. Potential reservoir rock. No type section nominated. Interpreted to be deltaic in origin. Correlated in part with the Arumbera Sandstone and Winnall beds. See also  p16, p17, p19. ||||Overlies the Julie Formation and unconformably overlies the Bitter Springs Formation. Overlain by the Ellis Sandstone, Sir Frederick Conglomerate.|Red-brown, rarely green, fine to medium grained, flaggy, micaceous sandstone and poorly exposed sandy siltstone. A medium grained sandstone with common trough cross beds, current ripples and mud pellets also occurs.|14-SEP-22
3647|Carnegie Formation|69673|6|Mentioned|p64 fig 53, p76, p88, p91|||Potential reservoir rock.||||Overlain by Sir Frederick Conglomerate, Ellis Sandstone, correlates with Arumbera Sandstone||
3647|Carnegie Formation|70416|5|Briefly described|p65 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||Basal Winnall Group.||Overlies Julie Formation. Is overlain by Ellis Sandstone.||
3647|Carnegie Formation|70793|4|Described|500k_interpgeop14_lut.csv|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|635-509 Ma (inferred)||||Siltstone, dolomite, diamictite, sandstone, and conglomerate|
3647|Carnegie Formation|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
3647|Carnegie Formation|70839|4|Described|p325,329-333,335,337-340,344|Ediacaran|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Thickness: typically <2000m, but reaches up to 3400m in one localised depocentre (Haines et al., 2012). SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Concordant ages between c. 0.82 and 1.78 Ga, single zircon age of c. 2.49 Ga. Dominant age components beween c. 1.22 and 1.08 Ga, smaller componetns between c. 1.36 and 1.28 Ga, and c. 1.78 and 1.68 Ga.|Max dep age: 819+\-13 Ma (238U/206Pb)|||Overlain by Ellis Sandstone and Sir Frederick Conglomerate. Underlain by Boord Formation/Julie Formation or Bitter Springs Formation. Correlable to unit 1 of the Winnall beds.|Red-brown sandstone, siltstone, and minor conglomerate.|
3647|Carnegie Formation|71080|5|Briefly described|p20,  p29 fig 20, p30|Ediacaran|Ediacaran|Amadeus Basin, WA. Arumberia locally common.  Supersequence 4.||||Equivalent to the Arumbera Sandstone.|Dominantly sandstone. Some shale.|04-FEB-19
3647|Carnegie Formation|71088|4|Described|p1-p2, p7-p8, p12, p15|Late Ediacaran|Cryogenian|Amadeus Basin. Reassigned to Supersequence 4. Considered partly equivalent to Cryogenian units. Originally correlated with the now sub-divided Boord Formation in WA and the Areyonga Formation and Inindia beds in the NT (Wells et al., 1970). Haines et al (2012) correlated it with the Arumbera Sandstone and lower Winnall beds which suggests a late ediacaran age. Sedimentary features include cross-beds, ripples, erosive sole marks including flutes and dessication cracks. Deposited in a deltaic environment. This formation is less than 2000m thick in most areas but reaches or exceeds 3400m in thickness in a depocentre west of Sir Frederick Range (Haines et al., 2012). Possible organic remains of unknown biostratigraphic significance are identified in a number of outcrops. Unconformably overlain by the Mu Formation. Equivalent to the Angas Hills Formation. See also p18-p21, p24, p33.||||Overlies the Julie Formation. Unconformably overlies the Bitter Springs Formation. Overlain by the Sir Frederick Conglomerate and (probably disconformably) by the Ellis Sandstone.|Immature, red-brown, fine- to medium-grained lithic and feldspathic sandstone and interbedded micaceous siltstone.|01-MAY-23
3647|Carnegie Formation|71114|5|Briefly described|p170 fig 1b|Ediacaran|Ediacaran|||||||
3647|Carnegie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, congloemrate, siltstone, sandstone|
3647|Carnegie Formation|71268|4|Described|GEOL_LUT_CSV files|Series 2|Ediacaran|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|635-510 Ma (inferred)||||Sandstone, siltstone, shale, conglomerate, diamictite, dolomite.|
3647|Carnegie Formation|71279|5|Briefly described|p355 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
3647|Carnegie Formation|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Julie Formation. Overlain by the Ellies Sandstone and the Sir Frederick Conglomerate.|Sandstone.|
3647|Carnegie Formation|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.||||Overlies Bitter Springs Group. Is overlain by Ellis Sandstone.|Fine- to medium-grained, cross-bedded, poorly-sorted, lithic and feldspathic red-brown sandstone; poorly exposed, micaceous red-brown siltstone (inferred to have been deposited during the Petermann Orogeny).|
3647|Carnegie Formation|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Overlain by Sir Frederick Conglomerate or Ellis Sandstone. Grades into Winnall beds. Underlain by Boord Formation.||
3647|Carnegie Formation|71842|4|Described|iii,p2-3,5,7-9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA). Exposed at the base of Mount Conner as several low sandstone ridges to the north.||Unit of Pertaoorrta Group.||Overlain by Sir Frederick Conglomerate or Ellis Sandstone. Underlain unconformably by Boord Formation or Julie Formation. Correlable to Arumbera Sandstone or Winnall beds.|Friable,felspathic and micaceous, fine-grained dark brown, occasionally red-tinged (ferruginised)  sandstone and occasional siltstone, cross-bedded clean, quartz sandstone.|
3647|Carnegie Formation|72034|5|Briefly described|500k_interpgeop16_lut|Series 2|Ediacaran|Amadeus Basin (Phase 1).|||||Quartz wacke, sandstone, siltstone, shale.|
3647|Carnegie Formation|72358|6|Mentioned|p118|Ediacaran|Ediacaran|Of Amadeus Basin.||||||
3647|Carnegie Formation|72360|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.|||||Sandstone, siltstone, pebbly sandstone and conglomerate.|09-SEP-19
3647|Carnegie Formation|72601|5|Briefly described|p3, p11-12, p14|Cambrian|Ediacaran|Amadeus Basin, western portion[?]. Previously mapped together with the Ellis Sandstone as the Winnall beds.||||Underlain, unconformably in part, by the Julie Formation. Equivalent to Mu Formation, Arumbera Sandstone and Winnall beds.||
3647|Carnegie Formation|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Conformably overlies the Julie Formation, disconformably underlies the Mount Currie Conglomerate.||
3650|Carnilya Hill ultramafics|39102|6|Mentioned|p81|||||||||
3661|Carpet Snake Syenogranite|24196|6|Mentioned|p44|||||||||
3661|Carpet Snake Syenogranite|24494|5|Briefly described|p21, p38 App.1|||||||||
3661|Carpet Snake Syenogranite|42904|5|Briefly described|map legend|||Reserved as Carpet Snake Complex||||||
3661|Carpet Snake Syenogranite|43215|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
3661|Carpet Snake Syenogranite|43234|6|Mentioned|p5|||||||||
3661|Carpet Snake Syenogranite|43478|2|Defined|p31-62|||||||||
3661|Carpet Snake Syenogranite|50075|5|Briefly described|p16|Archean|Archean|Geological Province: Yilgarn Craton.||||||23-DEC-09
3661|Carpet Snake Syenogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite-muscovite syenogranite.  Geological Province: Yilgarn Craton.||||||23-DEC-09
3661|Carpet Snake Syenogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Massive muscovite-biotite syenogranite; pegmatitic segregations.||||||07-FEB-11
3661|Carpet Snake Syenogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Massive muscovite-biotite syenogranite; pegmatitic segregations.|05-AUG-15
3661|Carpet Snake Syenogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2760 - 2642 Ma (inferred).||||Massive muscovite-biotite syenogranite; pegmatitic segregations.|
3661|Carpet Snake Syenogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenogranite|
3661|Carpet Snake Syenogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|2683-2642 Ma (inferred)||||Massive muscovite-biotite syenogranite; common pegmatitic segregations|
3663|Carr Boyd Group|22547|4|Described|p24||Ectasian|Geological province: Carr Boyd Basin.  Age: 1250 Ma. Overlain by Duerdin Group.||||||14-NOV-06
3663|Carr Boyd Group|22716|6|Mentioned|p237|Ectasian|Ectasian|Age: 1250 Ma. Regarded as equivalent to shallow marine deposits of Victoria River Basin.||||||
3663|Carr Boyd Group|22754|4|Described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|||||||
3663|Carr Boyd Group|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, ferruginous sandstone, siltstone and mudstone.  Age: c.1200Ma. Geological Province:Carr Boyd Basin.||||||22-MAY-08
3663|Carr Boyd Group|30097|6|Mentioned|Table 23|||Also Fig.54||||||
3663|Carr Boyd Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
3663|Carr Boyd Group|30892|6|Mentioned|Table 1|||Upper Proterozoic age||||||
3663|Carr Boyd Group|31393|6|Mentioned|Pl.25|||||||||
3663|Carr Boyd Group|32307|6|Mentioned|p10|||||||||
3663|Carr Boyd Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
3663|Carr Boyd Group|32660|4|Described|Table 6|||||||||
3663|Carr Boyd Group|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
3663|Carr Boyd Group|32728|6|Mentioned|p3|||||||||
3663|Carr Boyd Group|33377|6|Mentioned|p264|||||||||
3663|Carr Boyd Group|36885|3|Fully described|p178|||||||||
3663|Carr Boyd Group|36888|6|Mentioned|p213|||||||||
3663|Carr Boyd Group|36898|6|Mentioned|p183|||||||||
3663|Carr Boyd Group|37299|6|Mentioned|Fig.1|||||||||
3663|Carr Boyd Group|37462|4|Described|Table 4.VI|||See also Fig.4.13||||||
3663|Carr Boyd Group|38157|6|Mentioned|p282|||||||||
3663|Carr Boyd Group|40105|6|Mentioned|Fig.3|||||||||
3663|Carr Boyd Group|40494|6|Mentioned|p11|||||||||
3663|Carr Boyd Group|40765|6|Mentioned|p11|||||||||
3663|Carr Boyd Group|40813|6|Mentioned|p335|||||||||
3663|Carr Boyd Group|41158|5|Briefly described|p21|||Includes the Hensman Sandstone and Golden Gate Siltstone.  Mention 19.||||||04-APR-13
3663|Carr Boyd Group|41703|6|Mentioned|p232|||||||||
3663|Carr Boyd Group|41864|6|Mentioned|p64|||||||||
3663|Carr Boyd Group|42191|5|Briefly described|p439|||||||||
3663|Carr Boyd Group|43561|6|Mentioned|p1441|||||||||
3663|Carr Boyd Group|43595|6|Mentioned|p444|||||||||
3663|Carr Boyd Group|43666|6|Mentioned|p7|||||||||
3663|Carr Boyd Group|44140|6|Mentioned|p294|||Kimberley Basin. Ungrouped.||||Unconformably overlies Revolver Creek Formation.||
3663|Carr Boyd Group|44155|5|Briefly described|p232, p250, p253, p254 Fig.3-40|Mesoproterozoic|Mesoproterozoic|Total thickness 6km.|||Hensman and Stonewall Sandstones; Golden Gate Siltstone; Lissadell, Glenhill and Pincombe Formations; Bandicoot Range beds.|Correlated with Fitzmaurice Group in NT.|Sandstone, siltstone and shale.|
3663|Carr Boyd Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
3663|Carr Boyd Group|44363|4|Described|p.17|||(Adelaidean) units.||||||
3663|Carr Boyd Group|44364|14|Not recorded|map legend|||||||||
3663|Carr Boyd Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
3663|Carr Boyd Group|45047|4|Described|p33|||See also pp34,35. Adelaidean.||||||03-AUG-06
3663|Carr Boyd Group|45112|6|Mentioned|p34|||||||||
3663|Carr Boyd Group|45140|6|Mentioned|p13-14|||Kimberley region. Age range given as ?1200-?900 Ma.||||||
3663|Carr Boyd Group|46864|5|Briefly described|p40|||||||||
3663|Carr Boyd Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria River Basin.||||||07-FEB-11
3663|Carr Boyd Group|60533|5|Briefly described|p604|Mesoproterozoic|Mesoproterozoic|Sedimentary. ||||||
3663|Carr Boyd Group|64104|6|Mentioned|p75, p76 fig 10|Paleoproterozoic|Paleoproterozoic|Suggested source of sedimentary clasts in Duerdin Group in Texas/Mabel Downs and Purnululu area. [This article changes the age of a number of units, including this one, without explanation. Error in Figure 10?]||||||19-MAY-15
3663|Carr Boyd Group|64580|4|Described|map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, ferruginous sandstone, siltstone, and mudstone.||||||09-DEC-08
3663|Carr Boyd Group|64748|5|Briefly described|p275|Mesoproterozoic||Overlies the Bastion Group||||||
3663|Carr Boyd Group|65417|4|Described|pp156-167. |Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Exposed in Carr Boyd and Pincombe Ranges. No complete section is known due to extensive faulting; c.100 km of post-deposition strike-slip movement.  At least 4.4 km thick. Three main facies: shallow marine shelf, delta front, and braided delta plain. Sedimentation described in detail.|c.1200 Ma.||Includes Hensman and Stonewall Sandstones; Golden Gate Siltstone; Lissadell, Glenhill and Pincombe Formations.|Unconformably overlies Lamboo Complex. Is overlain unconformably by Duerdin Group.|Fine-grained clastics: sandstones and argillites.|
3663|Carr Boyd Group|69003|5|Briefly described|p5, p42, p44|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. With the Revolver Creek Formation, hosts the diamondiferous Argyle lamproite intrusion.|c.1200 Ma.|||||
3663|Carr Boyd Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin|||Includes Glenhill Formation, Lissadell Formation, Golden Gate Siltstone, Hensman Sandstone||sandstone, ferruginous sandstone, siltstone, and mudstone|
3663|Carr Boyd Group|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|||Includes Glenhill Formation, Lissadell Formation, Golden Gate Siltstone, Hensman Sandstone||Undivided; sandstone, ferruginous sandstone, siltstone and mudstone.|
3663|Carr Boyd Group|69435|5|Briefly described|p20:1-3, 5-6|||Carr Boyd Basin. Possible correlative of the Fitzmaurice Group. Thought to be Mesoproterozoic.|||Hensman, Stonewall Sandstones; Golden Gate Siltstone; Lissadell, Glenhill, Pincombe Formations.|||12-JUL-16
3663|Carr Boyd Group|69597|6|Mentioned|p2, p5 fig 2b, p55|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Black pyritic shales are the likely source of shallow high conductivities observed in the MT data. |c. 1200 Ma|||Unconformably overlies the Kimberley Group.|Black pyritic shales.|
3663|Carr Boyd Group|69634|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1200-1177 Ma (Inferred)||Include Glenhill Formation, Golden Gate Siltstone, Hensman Sandstone, Lissadell Formation.||Undivided; sandstone, ferruginous sandstone, siltstone, and mudstone|
3663|Carr Boyd Group|69673|6|Mentioned|p60 fig 48||||||Includes Hensman Sandstone, Golden Gate Siltstone, Lissadell Formation, Glenhill Formation, Stonewell Sandstone, Pincombe Formation|||
3663|Carr Boyd Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|1177-1200 Ma||Includes Glenhill Formation, Lissadell Formation, Golden Gate Siltstone, Hensman Sandstone||Sandstone, ferruginous sandstone, siltstone, and mudstone.|
3663|Carr Boyd Group|70731|6|Mentioned|p268,278|Stenian|Stenian|Geological province: King Leopold Orogen and Lamboo Province, Halls Creek Orogen, Kimberley Craton. Associated with Yampi Orogeny.||||||
3663|Carr Boyd Group|70812|6|Mentioned|p7|||||||||
3663|Carr Boyd Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin.||||||
3663|Carr Boyd Group|70851|5|Briefly described|p6, p17-p19, p29|||Eastern Zone, Lamboo Province.|c. 1200 Ma|||Overlies the Bastion Group. Overlain by the Antrim Plateau Volcanics.|Sedimentary rocks.|28-MAR-23
3663|Carr Boyd Group|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1200-1177 Ma (inferred)||Includes Glenhill Formation, Hensman Sandstone, Golden Gate Siltstone, Lissadell Formation, Bandicoot Range beds, Pincombe Formation, Stonewall Sandstone.|||
3663|Carr Boyd Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin.|||||Sandstone, ferruginous sandstone, siltstone, and mudstone.|
3663|Carr Boyd Group|73255|6|Mentioned|p533 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
3666|Carr Boyd Rocks Complex|24494|6|Mentioned|p20|||||||||
3666|Carr Boyd Rocks Complex|32694|3|Fully described|p1093|||See also pp1094-1113.||||||03-AUG-06
3666|Carr Boyd Rocks Complex|60076|5|Briefly described|p19|||Largely composed of pyroxenite; includes layered ultra mafic to mafic sequences, cross-cut by bronzitites.  Geological Province: Gindalbie domain (Yilgarn Craton).||||||02-FEB-05
3666|Carr Boyd Rocks Complex|65264|5|Briefly described|p16|||Composed largely of pyroxenite; includes layered ultramafic to mafic sequences (recognised in drillcore; Purvis et al 1972), crosscut by bronzites.||||||07-FEB-11
3677|Carranya Formation|41751|6|Mentioned|p8|||||||||
3677|Carranya Formation|44143|4|Described|p.426, p441 Table 4-19|Ordovician|Ordovician|Up to 135 m thick; sandstone and conglomerate; shallow marine. Correlates with part of Nambeet Formation. Contains Arenigian trilobites and gastropods. Type section in BILLILUNA, 19deg 10' S, 127deg 40' E approximately.||||||22-NOV-17
3677|Carranya Formation|64334|5|Briefly described|p38 Fig.2, p39-41, 44-46|Ordovician|Ordovician|Eastern Canning Basin. Tremadoc-Arenig. Detrital zircon analyses and plots; ages and provenances discussed.||||Correlates with Nambeet Formation and equivalents.|Sandstone and conglomerate; contains rare Early Ordovician macrofossils.|
3677|Carranya Formation|64580|4|Described|map legend||Ordovician|Sandstone and polymictic conglomerate, fossiliferous.||||||09-DEC-08
3677|Carranya Formation|64643|5|Briefly described|p3 Fig. 2|Middle Ordovician|Lower Ordovician|||||||
3677|Carranya Formation|65301|5|Briefly described|p5 Fig. 4|Middle Ordovician|Early Ordovician|Geological province: Canning Basin.||||||
3677|Carranya Formation|65449|5|Briefly described|p3, p6|Middle Ordovician|Early Ordovician||||||Sandy and conglomeratic (near basin margin) facies.|
3677|Carranya Formation|68007|6|Mentioned|p4|Ordovician|Ordovician|Canning Basin.||||||
3677|Carranya Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Early Ordovician|Early Ordovician|Canning Basin. See also 500k_geologyp08_lut.csv and GEOCHRON.csv (184260.1.pdf Wingate, 2007). U-Pb zircon (detrital) maximum deposition age.||548 +/- 7 Ma (Wingate, 2007)|||Sandstone and polymictic conglomerate, fossiliferous|27-NOV-15
3677|Carranya Formation|68902|6|Mentioned|p9 fig 5|Ordovician|Ordovician |||Prices Creek Group||||
3677|Carranya Formation|69099|5|Briefly described|500k_geologyp08_lut.csv||Ordovician||||||Sandstone and polymictic conglomerate, fossiliferous.|30-JUL-15
3677|Carranya Formation|69165|4|Described|500k_geologyp08_lut.csv|Ordovician|Ordovician||||||Sandstone and polymictic conglomerate; fossiliferous.|
3677|Carranya Formation|69182|6|Mentioned|Ch4 p3, Ch4 p9-p12|||Canning Basin. See also Ch4 p40-p41, Ch4 p45, Ch4 p47, Ch4 p50-p58, Ch4 p74, Ch4 p79-p82, Ch4 p92. ||||||
3677|Carranya Formation|69587|4|Described|GEOL_LUT_CSV files + geochron files|Early Ordovician|Early Ordovician|Of Canning Basin. Type section: outcrop on the east sde f Tanami Road, 15km W-NW of Carranya Homestead (MGA Zone 52, 358266E 7880557N). Restricted in outcrop to the Billiluna Shelf of the Canning Basin (Blake et al., 1977). Locally the basal unit of the Canning Basin succession and poorly preserved shelly fossils suggest an approximate Early Ordovician age. Sample GSWA 184269 (qtz sandstone) yielded a weighted mean 238U/206Pb* date of 548+\-7 Ma, a weighted mean 238U/206Pb* date of 548+\-7 Ma. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|485.4-470 Ma (biostrat)||||Sandstone and polymictic conglomerate; fossiliferous|
3677|Carranya Formation|70129|5|Briefly described|Map legend|Ordovician|Ordovician|Canning Basin.|||||Sandstone and polymictic conglomerate; fossiliferous (section only).|
3677|Carranya Formation|70142|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Canning Basin.|||||Sandstone and polymictic conglomerate, fossiliferous.|
3677|Carranya Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Lower Ordovician|Lower Ordovician||470-485 Ma||||Sandstone and polymictic conglomerate; fossiliferous|
3677|Carranya Formation|70774|5|Briefly described|p4|Middle Ordovician|Early Ordovician|Fitzroy Trough and Lennard Shelf, Canning Basin.||||||06-FEB-20
3677|Carranya Formation|71171|3|Fully described|p1-p2, p4-p10, p12-p14, p16-p18, p20|Ordovician|Ordovician|Crops out on the Billiluna Shelf and Balgo Terrace of the Canning Basin. Previouly assigned an Ordovician age. The type section is located 103km south of Halls Creek on Carranya Station and is obliquely crossed by the Tanami Road 14km west of the Wolfe Creek Meteorite Crater. Name derived from the Carranya Station. The type section was originally measured as being 150m thick. Measured sections at the type section and 13km west were logged between 107 and 135m. Petrography, outcrop localities, paleocurrent, sedimentary structures and fossil assemblage are discussed in detail. Unconformably overlies the Proterozoic basement originally mapped as Baines Beds but recently mapped as undivided Birrindudu Group. Time equivalent to the Goldwyer Formation.||Prices Creek Group||Unconformably overlies the Birrindudu Group. Unconformably overlain by the Grant Group.|Fine- to medium-grained quartz sandstone, pebble conglomerate and minor siltstone.|
3677|Carranya Formation|71267|4|Described|GEOL_LUT_CSV files|Early Ordovician|Early Ordovician|Events: Point Moody Extension (300-242 Ma); Red Bluffs Extension (372.2-360 Ma); Van Emmerick Extension (382.7-372.2 Ma); Samphire Marsh Extension (485-480 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|485.4-470 Ma (biostrat)||||Shallow marine fossiliferous fine to medium grained well sorted and laminated to thinly bedded quartz sandstone, siltstone, intraformational claystone conglomerate and pebble to boulder conglomerate|
3677|Carranya Formation|71894|5|Briefly described|p4|Lower Ordovician|Lower Ordovician|Canning Basin.||||Overlain by the Prices Creek Group.|Sandstone.|
3677|Carranya Formation|72034|5|Briefly described|500k_interpgeop16_lut|Early Ordovician|Early Ordovician|Canning Basin. Age from biostratigraphy.|||||Sandstone and polymictic conglomerate; fossiliferous.|
3677|Carranya Formation|72497|5|Briefly described|p3 Fig.2.|Early Ordovician|Early Ordovician|Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Unconformably underlies Willarar Formation and is laterally equivalent to Nambeet Formation.||
3677|Carranya Formation|72499|5|Briefly described|p7 Fig.6.|Early Ordovician|Early Ordovician|Located in the Fitzroy Trough.||||Underlies Prices Creek Group.|Includes sandstone.|
3677|Carranya Formation|72503|6|Mentioned|p26|||Canning Basin. Crops out along the Billiluna Shelf.||||Equivalent[?] to Goldwyer Formation.||
3677|Carranya Formation|73117|5|Briefly described|p3|Middle Ordovician|Middle Ordovician|Canning Basin.||||Unconformably underlain[?] by Prices Creek Group.|Dominantly sandstone with lesser conglomerate.|
3677|Carranya Formation|73344|6|Mentioned|p4, p6|Middle Ordovician|Middle Ordovician|Canning Basin. Observed in outcrop. Was originally believed to be laterally equivalent to the Wilson Cliffs Sandstone, Nambeet Formation and Kunian Sandstone. Part of supersequence A2.||||Equivalent to Goldwyer Formation.||
3677|Carranya Formation|73346|5|Briefly described|p1-3, p4, p27, p30|Ordovician|Ordovician|Canning Basin, Billiluna Shelf (surface outcrops occur in this region). Poorly dated based on limited paleontological data. Shallow marine (tidal) to fluvial origin.|||||Fine- to medium-grained quartz sandstone, pebble conglomerate and minor siltstone.|
3686|Carribuddy Group|1943|5|Briefly described|p384|||Canning Basin. Upper part correlated with Ajana Formation, Carnarvon Basin.||||||
3686|Carribuddy Group|13255|6|Mentioned|p368|Late Silurian|Middle Ordovician|Roebuck Basin.||||Overlies Nita Formation. Is overlain by Tandalgoo Formation.||
3686|Carribuddy Group|14228|5|Briefly described|p6 fig3|Silurian|Ordovician|[Mis-spelt as Carrabuddy]. South Canning Basin.|||Sahara Formation, Mallowa Salt, Nibil Formation, Minjoo Salt, Bongabinni Formation.|Overlies Nita Formation||05-OCT-16
3686|Carribuddy Group|22646|6|Mentioned|Fig 5 on p 105|Late Ordovician|Early Ordovician|Canning Basin.||||||
3686|Carribuddy Group|22650|5|Briefly described|p 164|Early Devonian|Silurian|Province - Canning Basin.||||||
3686|Carribuddy Group|22753|5|Briefly described|Fig.3 p585|Silurian|Ordovician|||||||
3686|Carribuddy Group|22814|5|Briefly described|p256, fig2|Late Silurian|Late Ordovician|||||||
3686|Carribuddy Group|23377|6|Mentioned|p210|Devonian|Silurian|of Canning Basin.||||||
3686|Carribuddy Group|24449|5|Briefly described|p745, p741 Fig. 2|Wenlockian|Llanvirnian|Geological Province: Canning Basin.||||||
3686|Carribuddy Group|40617|6|Mentioned|p3|||||||||
3686|Carribuddy Group|40837|2|Defined|p257 Fig. 4, p273|Early Devonian|Early Devonian|Supersedes Carribuddy Fm. Contains Bongabinni Fm, Minjoo Salt, Mallowa Salt, Sahara Fm replacing informally named Units A, B, C, D, E of Carribuddy Formation. Overlain by Worral Fm; overlies Nita Fm. Thickness: 1591m. See also Fig. 5 page insert (p258).||||||27-JAN-10
3686|Carribuddy Group|40992|6|Mentioned|Fig.11|||||||||
3686|Carribuddy Group|41215|6|Mentioned|Fig.4|||||||||
3686|Carribuddy Group|41271|6|Mentioned|p39|||||||||
3686|Carribuddy Group|41730|6|Mentioned|p472|||||||||
3686|Carribuddy Group|42030|5|Briefly described|p747|||||||||
3686|Carribuddy Group|42338|5|Briefly described|p144|||||||||
3686|Carribuddy Group|42441|6|Mentioned|p84|||Canning Basin||||||
3686|Carribuddy Group|42442|6|Mentioned|p6|||Canning Basin||||||
3686|Carribuddy Group|42792|5|Briefly described|p223|||||||||
3686|Carribuddy Group|42933|5|Briefly described|Fig.94 p258|||||||||
3686|Carribuddy Group|43563|6|Mentioned|Fig.2,p4|||||||||
3686|Carribuddy Group|43599|6|Mentioned|p247|||||||||
3686|Carribuddy Group|43803|6|Mentioned|Fig.5,p71||Llanvirnian|||||||
3686|Carribuddy Group|43818|6|Mentioned|Fig.2.p39||Silurian|||||||
3686|Carribuddy Group|44143|4|Described|p428, p440-441 Tb. 4-19, p442 Fig.4-96|Devonian|Late Silurian|Includes Bongabinna, Mount Troy, Nibil and Sahara Formations; Minjoo and Mallowa Salts. Halite, dolomite, siltstone, claystone, shale. Is overlain unconformably by Worral Formation.||||||22-NOV-17
3686|Carribuddy Group|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Canning Basin.||||||
3686|Carribuddy Group|61021|5|Briefly described|p36 Fig. 2|Silurian|Ordovician|Includes the Bongabinni Formation. Overlies the Nita Formation. Geological Province: Canning Basin.||||||17-DEC-07
3686|Carribuddy Group|61023|5|Briefly described|p10 Fig. 6|Silurian|Ordovician|Of marginal marine to non-marine origin; evaporitic. Geological Province: Canning Basin.||||||10-APR-08
3686|Carribuddy Group|61139|5|Briefly described|p42|Silurian|Ordovician|Geological Province: Canning Basin.||||||09-JUN-05
3686|Carribuddy Group|61551|5|Briefly described|p359.|Silurian|Ordovician|Canning Basin. Forms a seal for hydrocarbons sourced from the Goldwyer Formation. Up to 1500m thick, of which one third is massive evaporite facies.|||Includes Nibil and Bongabinni Formations, and Mallowa and Minjoo Salts.||Shale, kerogenous shale, impermeable carbonate, and evaporite facies.|
3686|Carribuddy Group|62982|5|Briefly described|p7|Silurian|Llanvirnian|Red bed mudstone and dolostone facies dominate and thick halite deposits developed in sub-basins; largely devoid of diagnostic fossils. Algal oil shales present in basal parts. Geological Province: Canning Basin.||||Overlies Nita Formation||19-JAN-10
3686|Carribuddy Group|64334|5|Briefly described|p39-43|Silurian|Ordovician|Canning Basin; subsurface only. Marginal marine and evaporitic. Caradoc - ?Pridoli. Generally devoid of age-diagnostic fossils.|||Bongabinni, Mount Troy, Nibil, Sahara Formations; Minjoo, Mallowa Salts.|Overlies Nita Formation.|Mainly mudstone; halite, dolostone.|
3686|Carribuddy Group|64643|5|Briefly described|p3 Fig. 2|Llandovery|Middle Ordovician|||||||
3686|Carribuddy Group|64982|5|Briefly described|p699 Fig.4.|Llandovery|Ashgill||||Includes Mallowa and Minjoo Salts; Sahara, Bongabinni, Mount Troy and Nibil Formations.|||
3686|Carribuddy Group|65301|5|Briefly described|p3, p5 Fig. 4|Silurian|Late Ordovician|Conformably overlain by Worral Formation. Geological province: Canning Basin, including Kidson Sub-basin and Broome Platform. Succession of marginal marine to non-marine mudstone, minor dolomite, and sandstone.||||||
3686|Carribuddy Group|65449|3|Fully described|p1-60; Plates 1, 6-7, 11|Llandovery|Darriwilian|Canning Basin. Originally named the Carribuddy Formation (Singleton, 1965); defined by Koop (1966). Redefined as Carribuddy Group, with six named Formations, by Lehmann (1984): 5 of their type sections are in Kidson 1. No outcrop. In absence of salt units, subdivision of the Group is difficult because of repetitive facies and lack of biostratigraphic data. At least 1591m thick. A regional seal to the prospective Larapintine 2 petroleum system. Has potential sandstone and carbonate reservoirs locally. Deposition mostly in supratidal environments; periodic halite-dominated deposition in salterns. Details of petroleum wells/mineral drillholes intersecting this unit. Biostratigraphic data detailed.|||Includes Bongabinni, Mount Troy, Nibil and Sahara Formations; Minjoo and Mallowa Salts.|Overlies Nita Formation conformably (locally unconformably) and Goldwyer Formation. Is overlain conformably by Worral Formation and unconformably by Grant Group.|Marginal marine and evaporitic sediments: halite; redbed mudstone, dolomitic or calcareous in part; minor sandstone and carbonate interbeds.|24-FEB-20
3686|Carribuddy Group|66949|6|Mentioned|p73 Appx.5|Silurian|Silurian|||||||05-OCT-16
3686|Carribuddy Group|68007|3|Fully described|p1, p4, p6, p11-15, Plates 1, 2|Early Silurian|Late Ordovician|Canning Basin. About 927m thick in Patience 2 well. A thick marginal marine succession of fine siliciclastic and carbonate rocks commonly interbedded with thick halite-dominated evaporite Formations. Reference section is in Kidson 1 well. Potential for salt to form an effective hydrocarbon seal. Composite well log.|||Includes Bongabinni Formation, Minjoo Salt, Mallowa Salt, Pegasus Dolomite Member.|Conformably overlies Nita Formation. Is overlain conformably or paraconformably by the Worral Formation.|Dark reddish-brown claystone and siltstone, variably dolomitic, with minor greenish grey horizons or mottles, occasional anhydrite.|24-FEB-20
3686|Carribuddy Group|68902|6|Mentioned|p9|Silurian|Late Ordovician||||Includes Bongabinni Formation, Nibil Formation, Sahara Formation|Is overlain by Worral Formation.||18-JAN-17
3686|Carribuddy Group|69029|5|Briefly described|p320|||Of Canning Basin. Salt-dominant successions; salt units have excellent sealing capacities. Interpreted to have been favourable affected by tectonics for trap development during Early Ordovician extension, and Permian-Triassic cooling events (Ghori and Haines, 2006b).||||Overlies the Nita Formation and the Wallara Formation.||04-SEP-19
3686|Carribuddy Group|69182|5|Briefly described|Ch4 p9-p12, Ch4 p20-p25|Llandovery|Upper Ordovician|Canning Basin. See also Ch4 p30-p36, Ch4 p38-p41, Ch4 p44, Ch4 p45, Ch4 p47-p48, Ch4 p50-p58, Ch4 p64-p65, Ch4 p74, Ch4 p79-p82, Ch4 p87, Ch4 p92, Ch4 p94. |||Includes the Bongabinni Formation, Minjoo Salt, Mallowa Salt, Nibil Formation and the Sahara Formation.|Overlies the Nita Formation. Overlain by the Worral Formation.|Red-bed succession of dolomites, claystones, sandstones and salts.|
3686|Carribuddy Group|69297|6|Mentioned|p350|Silurian|Late Ordovician|Canning Basin. |||Includes the Bongabinni Formation.|||
3686|Carribuddy Group|69312|6|Mentioned|p3|Llandovery|Middle Ordovician|Canning Basin. Misspelt as the Carrabiddy Group on p15. |||Includes the Bongabinni Formation, Minjoo Salt, Nibil Formation, Mallowa Salt and Sahara Formation.|Overlies the Nita and Goldwyer Formations. Overlain by the Worral Formation.||11-FEB-20
3686|Carribuddy Group|69883|5|Briefly described|p1, p4-p6, p14, p21, p45|Llandovery|Middle Ordovician|Canning Basin. Deposited in a marginal marine to non-marine environment. This group is only preserved locally within sub-basin depocentres.|||Includes the Bongabinni Formation, Mount Troy Formation, Minjoo Salt, Nibil Formation, Mallowa Salt and the Sahara Formation.|Overlies the Nita Formation.||
3686|Carribuddy Group|70774|5|Briefly described|p4|Llandovery|Middle Ordovician|Willara and Kidson Sub-basins, Canning Basin.|||Includes the Minjoo and Mallowa Salts, the Nibil, Bongabinni and Sahara Formations.|Overlies the Nita Formation. Overlain by the Worral Formation.||
3686|Carribuddy Group|71146|5|Briefly described|p6, p45|Llandovery|Middle Ordovician|Canning Basin.|||Includes the Minjoo and Mallowa Salts.|Overlies the Nita Formation. Overlain by the Worral Formation.|Siltstone and evaporites.|
3686|Carribuddy Group|71171|5|Briefly described|p2|||Canning Basin.|||Includes the Bongabinni Formation, Minjoo Salt, Mount Troy Formation, Nibil Formation, Mallowa Salt and Sahara Formation.|||
3686|Carribuddy Group|71870|5|Briefly described|p3|Pridoli|Sandbian|Canning Basin.|||Includes the Bongabinni Formation, Minjoo Salt, Nibil Formation, Mallawa Salt and the Sahara Formation.|Overlies the Nita Formation. Overlain unconformably by the Tandalgoo Sandstone and Worral Formation.||
3686|Carribuddy Group|71894|5|Briefly described|p4, p20|Llandovery|Upper Ordovician|Canning Basin.|||Includes the Bongabinni Formation, Nibil Formation, Sahara Formation, Minjoo Salt and Mallowa Salt.||Shale and salts.|
3686|Carribuddy Group|72497|5|Briefly described|p3 Fig.2.|Late Silurian|Middle Ordovician|Shown as occuring in the Anketell, Tabletop, Ryan Shelves, Willara and Kidson Sub-basins, the Jurgurra and Barbwire Terraces and Broome Platform.|||Includes Sahara Formation, Mallowa Salt, Nibil Formation, Minjoo Salt, Mount Troy Formation and Bongabinni Formation.|Conformably overlies Goldwyer and Nita Formations. Unconformably overlain by Tandalgoo, Worral Formations.||
3686|Carribuddy Group|72499|5|Briefly described|p7 Fig.6.|Llandovery|Late Ordovician|Located in the Willara Sub-basin and Broome Platform.|||Includes Sahara Formation, Mallowa Salt, Nibil Formation, Minjoo Salt, Bongabinni Formation.||Includes shale, carbonate and evaporites.|
3686|Carribuddy Group|72504|6|Mentioned|Figure 3|Devonian|Silurian|Canning Basin, Broome Platform. Intersected in Pictor 1, Canopus 1, Looma 1, Robert 1, Fruitcake 1, Missing 1, Sally May 2 drillholes.||||||18-MAR-20
3686|Carribuddy Group|73117|5|Briefly described|p3, p114, p141-142|Llandovery|Upper Ordovician|Canning Basin.|||Sahara Formation, Mallowa Salt, Nibil Formation, Minjoo Salt, Bongabinni Formation.|Underlain by Nita Formation. Overlain by Worral Formation. Equivalent to Cobb Formation. Unconformably overlain by Grant Group.|Dominantly shale and mudstone.|
3686|Carribuddy Group|73344|6|Mentioned|p6|Pridoli|Darriwilian|Canning Basin, subsurface. Constitutes supersequence B.|||Sahara Formation, Mallowa Salt, Nibil Formation, Minjoo Salt, Mount Troy Formation, Bongabinni Formation|Underlain by Nita Formation.||
3686|Carribuddy Group|73345|6|Mentioned|p227|||Canning Basin, widespread. Potentially correlative to Barnicarndy Formation.||||||
3686|Carribuddy Group|73346|6|Mentioned|p3, p27, App.1 p34|Silurian|Late Ordovician|Canning Basin. Paralic and evaporative.|||Nibil Formation, Bongabinni Formation||Includes locally thick evaporite deposits.|
3696|Carson Volcanics|22440|6|Mentioned|p5|||||||||
3696|Carson Volcanics|22716|6|Mentioned|p236|Paleoproterozoic|Paleoproterozoic|Durack Ranges||||||07-NOV-08
3696|Carson Volcanics|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.||||||07-NOV-08
3696|Carson Volcanics|22814|6|Mentioned|p254|Proterozoic|Proterozoic|||||||
3696|Carson Volcanics|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Kimberley Group.||||||
3696|Carson Volcanics|23328|6|Mentioned|1031 Fig.2, 1033|||Geochemistry given for comparison.||||||07-SEP-09
3696|Carson Volcanics|23383|5|Briefly described|p19,  p18 Tb. 2|||Of Kimberley Group. Metabasalt, quartz sandstone, feldspathic sandstone, siltstone.  Conformably underlies Warton Sandstone; conformably overlies King Leopold Sandstone. Max thickness: 400 m. Geological Province: Kimberley Basin.||||||21-JUL-15
3696|Carson Volcanics|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Kimberley Group. Green to black basalt, amygdaloidal basalt, and basaltic volcaniclastic rocks; interbedded quartz sandstone, feldspathic sandstone, and laminated siltstone and mudstone. Geological Province: Kimberley Basin.||||||21-JUL-15
3696|Carson Volcanics|23621|4|Described|p31|Paleoproterozoic|Paleoproterozoic|Of Kimberley Group. Underlying unit King Leopold Sandstone. Geological Province: Kimberley Basin. Max. thickness: ~400 m.||||||07-NOV-08
3696|Carson Volcanics|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Basin.||||||07-NOV-08
3696|Carson Volcanics|23722|4|Described|p19|Paleoproterozoic|Paleoproterozoic|Max. thickness: 1140m.   Geological Province: Kimberley Basin||||||07-NOV-08
3696|Carson Volcanics|24173|4|Described|p23, p11 Tb.2|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group. Basalt lavas, minor sandstone. Conformably overlies King Leopold Sandstone. Geological Province: Kimberley Basin. Max Thickness: 400m.||||||07-NOV-08
3696|Carson Volcanics|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Basalt, amygdaloidal basalt, basaltic volcaniclastic rock, sandstone, siltstone and mudstone.  Geological Province: Kimberley Basin.||||||21-JUL-15
3696|Carson Volcanics|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Age: c.1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
3696|Carson Volcanics|29380|4|Described|p8|||On Table2, Carpentarian.||||||
3696|Carson Volcanics|29693|6|Mentioned|p106|||||||||
3696|Carson Volcanics|29946|6|Mentioned|Fig.1|||||||||
3696|Carson Volcanics|30097|6|Mentioned|p151|||Also Table 23||||||
3696|Carson Volcanics|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|Part of Kimberley Group||||||
3696|Carson Volcanics|30533|4|Described|p18|||See Table 3||||||
3696|Carson Volcanics|30636|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|30893|6|Mentioned|p205|||Carpentarian age. Lithology||||||
3696|Carson Volcanics|30894|5|Briefly described|p250|||Carpentarian age||||||
3696|Carson Volcanics|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|30896|4|Described|p16|||||||||
3696|Carson Volcanics|30897|5|Briefly described|p12|||Stratigraphy||||||
3696|Carson Volcanics|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3696|Carson Volcanics|31404|6|Mentioned|Fig.1|||||||||
3696|Carson Volcanics|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
3696|Carson Volcanics|31565|5|Briefly described|p970|||||||||
3696|Carson Volcanics|31662|6|Mentioned|Fig. 1|||||||||
3696|Carson Volcanics|32108|6|Mentioned|p231|||||||||
3696|Carson Volcanics|32660|5|Briefly described|Table 3|||||||||
3696|Carson Volcanics|32662|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|32663|4|Described|Table 1|||Carpentarian||||||
3696|Carson Volcanics|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
3696|Carson Volcanics|32728|5|Briefly described|p38|||||||||
3696|Carson Volcanics|33443|6|Mentioned|p260|||||||||
3696|Carson Volcanics|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|34137|4|Described|Table 1||Carpentarian|Carpentarian, part of Kimberley Group.||||||
3696|Carson Volcanics|34190|4|Described|Table 1|||Proterozoic||||||
3696|Carson Volcanics|34462|4|Described|Table 1|||Carpentarian||||||
3696|Carson Volcanics|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
3696|Carson Volcanics|36551|4|Described|p34|||||||||
3696|Carson Volcanics|36885|6|Mentioned|p178|||||||||
3696|Carson Volcanics|37228|6|Mentioned|Fig.2|||||||||
3696|Carson Volcanics|37299|6|Mentioned|Fig.1|||||||||
3696|Carson Volcanics|37462|6|Mentioned|Fig.4.9|||||||||
3696|Carson Volcanics|37643|6|Mentioned|p5.5.2|||||||||
3696|Carson Volcanics|38071|6|Mentioned|p104|||||||||
3696|Carson Volcanics|38632|6|Mentioned|p21|||||||||
3696|Carson Volcanics|38988|6|Mentioned|p14|||||||||
3696|Carson Volcanics|39116|6|Mentioned|p134|||||||||
3696|Carson Volcanics|41158|6|Mentioned|p20|||See also Fig.9||||||
3696|Carson Volcanics|41453|6|Mentioned|p243|||||||||
3696|Carson Volcanics|41703|6|Mentioned|Fig.2|||||||||
3696|Carson Volcanics|41987|5|Briefly described|Fig.4 P74|||||||||
3696|Carson Volcanics|42149|6|Mentioned|Table 1 P709|||||||||
3696|Carson Volcanics|42186|6|Mentioned|p390|||||||||
3696|Carson Volcanics|42710|5|Briefly described|map legend|Proterozoic||||||||
3696|Carson Volcanics|42811|5|Briefly described|p22|||of Kimberley Group||||||
3696|Carson Volcanics|42814|4|Described|p13|||of Kimberley Group||||||
3696|Carson Volcanics|42815|5|Briefly described|map|Proterozoic||||||||
3696|Carson Volcanics|42821|6|Mentioned|p135|||||||||
3696|Carson Volcanics|42977|5|Briefly described|p275|||||||||
3696|Carson Volcanics|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Group.||||||
3696|Carson Volcanics|43661|6|Mentioned|p6||Proterozoic|||||||
3696|Carson Volcanics|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
3696|Carson Volcanics|44140|5|Briefly described|p295, p298, p300, p304|Paleoproterozoic|Paleoproterozoic|60-1140 m thick. Deformed c.600 Ma.||Kimberley Group|||Tholeiitic basalt, feldspathic sandstone, siltstone, chert; basalt commonly altered to spilite|07-MAR-18
3696|Carson Volcanics|44155|6|Mentioned|p250, p253|||Includes amphibolite from low-grade metamorphisn in King Leopold Orogen. Mentioned as possible correlate of Ninety Seven Mile Beds.||Kimberley Group||||
3696|Carson Volcanics|44230|5|Briefly described|Map Legend||Proterozoic|||||||
3696|Carson Volcanics|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group. Green to black basalt, amygdaloidal basalt and basaltic volcanic rocks, interbedded quartz sandstone, feldspathic sandstone, laminated siltstone and mudstone.  Geological Province: Kimberley Basin.||||||07-NOV-08
3696|Carson Volcanics|44286|5|Briefly described|Map legend|||||||||
3696|Carson Volcanics|44324|14|Not recorded|p.10||Carpentarian|Tb.2. (Carpentarian).||||||
3696|Carson Volcanics|44325|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
3696|Carson Volcanics|44363|5|Briefly described|p.6,11,12,13,15,27|||(Carpentarian) Kimberley Group.||||||
3696|Carson Volcanics|44364|14|Not recorded|map legend|||||||||
3696|Carson Volcanics|44366|14|Not recorded|p.15||Carpentarian|Part of Kimberley Group.||||||
3696|Carson Volcanics|44367|14|Not recorded|map legend|||(Reprinted 1971), part of Kimberley Group.||||||
3696|Carson Volcanics|44397|14|Not recorded|p.17,20,21, Table 2||Carpentarian|Kimberley Group.||||||
3696|Carson Volcanics|44398|14|Not recorded|map legend||Carpentarian|||||||
3696|Carson Volcanics|44694|5|Briefly described|Map Legend||Proterozoic|||||||
3696|Carson Volcanics|45047|5|Briefly described|p28|||Kimberley Group.||||||
3696|Carson Volcanics|45077|6|Mentioned|p7|||||||||
3696|Carson Volcanics|45087|5|Briefly described|p151|||Chem. analyses.||||||
3696|Carson Volcanics|48931|3|Fully described|p51|||||||||
3696|Carson Volcanics|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Mafic. Of the Kimberley Group. Geological Province: Kimberley Basin.||||||07-NOV-08
3696|Carson Volcanics|60714|5|Briefly described|p111, p113 Fig.2. |Statherian|Statherian|270 - 700 m thick. Rb-Sr whole-rock age of 1807 Ma (Bennett et al. 1975).|1790 +/- 4 Ma (magmatic zircon).|Unit in Kimberley Group.||Overlies King Leopold Sandstone. Is intruded by Hart Dolerite: may be coeval with the Hart Dolerite. Is overlain by Warton Sandstone.|Submarine, tholeiitic basalts.|
3696|Carson Volcanics|60724|5|Briefly described|p17|||Unconformably overlies the Lamboo Complex.||||||21-JUL-15
3696|Carson Volcanics|61571|5|Briefly described|p656, p657 Fig. 4|Paleoproterozoic|Paleoproterozoic|Thick basalts. Overlain by Warton Sandstone; overlies King Leopold Sandstone. Geological Province: Kimberley Basin.||||||21-JUL-15
3696|Carson Volcanics|62715|5|Briefly described|p1753|||Tholeiitic basaltic lavas.  Overlie King Leopold Sandstone.||||||
3696|Carson Volcanics|63866|5|Briefly described|p133|||Western Zone, Halls Creek Orogen.||Kimberley Group|||Basalt, basaltic volcaniclastics, amygdaloidal basalt and minor siltstone and sandstone.|
3696|Carson Volcanics|64580|4|Described|map legend||Paleoproterozoic|Of Kimberley Group. Basalt, amygdaloidal basalt, basaltic volcaniclastic rock, sandstone, siltstone, and mudstone.||||||09-DEC-08
3696|Carson Volcanics|64589|6|Mentioned|sample_locations file|||Sample locations.||||||
3696|Carson Volcanics|64748|4|Described|p269 Fig 2, Tb.1, p268,270,274-5,278|||Of the Kimberley Group.Overlies the King Leopold Sandstone.Underlies the Warton Sandstone. Tholeiitic basalts (mostly altered to spilite) with rhyolitic tuff, feldspathic sandstone siltstone and chert; 60-1140m thick;||||||21-SEP-18
3696|Carson Volcanics|66526|5|Briefly described|p13, p21.|||Kimberley Province of the Hart Large Igneous Province.|||||Basaltic lavas.|
3696|Carson Volcanics|67563|5|Briefly described|p120, p120 Fig.1, p122 Fig.2|Statherian|Statherian|Magmatic zircon age by Page and Sun (1994) refers to the Hart Dolerite which intrudes the Carson Volcanics, providing a minimum age.|1790 +/ 4 Ma|Of the Kimberley Group.||||20-JAN-17
3696|Carson Volcanics|67888|6|Mentioned|p15 fig 12, p106|Proterozoic|Proterozoic|||||||
3696|Carson Volcanics|68078|4|Described|p1, p4 figure 2|Paleoproterozoic|Paleoproterozoic|See also p6 figure 3, p14 figure 10, p21 figure 14, p24. ||Kimberley Group||Overlies King Leopold Sandstone, Overlain by Warton Sandstone, Intruded by Hart Dolerite|Tholeiitic basalt, volcaniclastic sandstone and breccia interbedded with feldspathic sandstone, quartz sandstone, siltstone and mudstone.|
3696|Carson Volcanics|68244|5|Briefly described|p661-662, p666|Late Paleoproterozoic|Late Paleoproterozoic|Kimberley Basin. Records glacially striated pavement is preserved.||Unit of Kimberley Group.||Unconformably overlain by the Landrigan Formation.||21-JUN-19
3696|Carson Volcanics|68473|6|Mentioned|p533|||||||||
3696|Carson Volcanics|68992|5|Briefly described|p498 Fig.1|Statherian|Statherian|Kimberley Basin. Magmatic zircon age.  |1790 +/- 4 Ma (Page and Sun,1994).|Of the Kimberley Group.||||
3696|Carson Volcanics|69003|5|Briefly described|p20-21|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Volcanic and volcaniclastic rocks.|
3696|Carson Volcanics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin||Kimberley Group|Includes unnamed sandstone member.|Conformably overlain by Warton Sandstone. Intruded by Hart Dolerite.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone, and mudstone|21-JUL-15
3696|Carson Volcanics|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.||Kimberley Group|||Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, silstone and mudstone.|
3696|Carson Volcanics|69585|5|Briefly described|p3-5, p27, p31|Statherian|Statherian|Possibly comagmatic with Hart Dolerite. Shows evidence of submarine extrusion (local occurrence of pillow structures).||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain conformably by Warton Sandstone.|Regionally extensive tholeiitic flows.|
3696|Carson Volcanics|69597|5|Briefly described|p3, p4, p6, p8 fig 4, p70 fig 57|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. 400-1100m thick. Contains locally disseminated sulfides. Dominates the magnetic response of the Kimberley along with the Hart Dolerite. Complicates interpretation of gravity data for the region.   |c. 1800 ma||||Tholeiitic basalts interlayered with sandstone, siltstone and chert.|
3696|Carson Volcanics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.  See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv250k_interpgeop_lut.csv and geochron files.|1835-1797 Ma (Inferred)|Unit of Kimberley Group.||Overlain conformably by Warton Sandstone. Intruded by Hart Dolerite.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone, and mudstone|
3696|Carson Volcanics|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, Kimberley Craton.||Unit in Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and mudstone.|
3696|Carson Volcanics|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin; North Australian Craton. An un-named subunit comprising feldspathic sandstone, quartz sandstone, and siltstone; lesser stromatolitic chert is mapped separately.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and chert.|
3696|Carson Volcanics|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. A facies association of feldspathic sandstone, quartz sandstone, siltstone and lesser stromatolitic chert is mapped separately.||Lower Kimberley Group (Kimberley Group).||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and chert.|04-NOV-15
3696|Carson Volcanics|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1797-1835 Ma|Kimberley Group|||Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone, chert and stromatolitic chert.|
3696|Carson Volcanics|70731|6|Mentioned|p270-271,273-274,276,278|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.  Intraplate mafic magmatism; associated with the Hart Dolerite, forming a LIP. Represents cessation of collisional tectonics after the end of Halls Creek Orogeny.||||||
3696|Carson Volcanics|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. An un-named sub-unit of feldspathic sandstone, quartz sandstone, and siltstone, with lesser stromatolitic chert, is mapped separately.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and chert.|
3696|Carson Volcanics|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. An un-named sub-unit of feldspathic sandstone, quartz sandstone, and siltstone, with lesser stromatolitic chert, is mapped separately.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and chert.|
3696|Carson Volcanics|70812|5|Briefly described|p6, p9, p31|Statherian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. Together with the Hart Dolerite is inferred to be part of a LIP.|c. 1800 Ma|Kimberley Group, Lower||Intruded by the Hart Dolerite.||
3696|Carson Volcanics|70851|4|Described|p4-p5, p9, p11, p18|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Rock properites are discussed. See also p20, p24, p29-p30, p34.|c. 1800-1775 Ma|Kimberley Subgroup, Lower||Overlies the King Leopold Sandstone. Overlain by the Warton Sandstone (Kimberley Subgroup, Upper). Intruded by the Hart Dolerite.||
3696|Carson Volcanics|71113|6|Mentioned|p102|Statherian|Statherian|Geological province: Lamboo Province, Halls Creek Orogen. May form part of a LIP marking the end of major magmatism in the Lamboo Province.||||||
3696|Carson Volcanics|71140|6|Mentioned|p102|Statherian|Statherian|With Hart Dolerite, marks the end of major magmatism in the Lamboo Province, Halls Creek Orogen.|c.1797 Ma.|||||
3696|Carson Volcanics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological provice: Halls Creek Orogen; King Leopold Orogen. Of Kimberley Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv and geochron files.|1835-1797 Ma (inferred)|Unit of Kimberley Group.||Intruded by Hart Dolerite. Overlain conformably by Warton Sandstone.|Green to black quartz basalt, in places amygdaloidal and with basaltic volcaniclastic rocks, interbedded massive feldspathic or argillaceous quartz sandstone, laminated siltstone and mudstone|
3696|Carson Volcanics|71281|4|Described|p421, p423, p430|Paleoproterozoic|Paleoproterozoic|Smith and Gemuts (1967). Kimberley Basin. Up to 1400m thick.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone. Is intruded by Hart Dolerite.|Green to black quartz basalt, in places amygdaloidal and volcaniclastic, interbedded with massive feldspathic or argillaceous quartz sandstone, laminated siltstone and mudstone.|
3696|Carson Volcanics|71784|6|Mentioned|p86|||||||||
3696|Carson Volcanics|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton. Mapped separately is an un-named subunit of feldspathic sandstone, quartz sandstone, and siltstone; localized stromatolitic chert.||Kimberley Group.||Overlies King Leopold Sandstone. Is overlain by Warton Sandstone and unconformably by Walsh Tillite.|Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone and chert.|
3696|Carson Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group, lower|||Massive and amygdaloidal basalt and basaltic volcaniclastic rock; interbedded quartz sandstone, feldspathic sandstone, siltstone, and chert.|
3696|Carson Volcanics|72437|5|Briefly described|p12, p115, p117|||Around 400m thick, described by Roberts et al, (1965). Eleven whole rock analyses of basalts are presented from the King Leopold Orogen.||basal Kimberley Group|||Massive and amygdaloidal basalt, basaltic volcaniclastic rock, interbedded sedimentary rock.|
3696|Carson Volcanics|72490|5|Briefly described|p2-5, p11-12|||||Kimberley Group||Intruded by Hart Dolerite.|Green to black, locally amygdaloidal basalt and basaltic volcaniclastic rocks with interbeds of feldspathic or argillaceous quartz sandstone, laminated siltstone and mudstone.|
3696|Carson Volcanics|73089|6|Mentioned|p40|Statherian|Orosirian|Kimberley Basin. Similar in age to 1817-1788 Ma granitic rocks in the southern Halls Creek Orogen. Comprise part of the voluminous (300 000 km3) Hart-Carson large igneous province.|[c. 1800 Ma?]|||Coeval with Hart Dolerite.||
3707|Cartier Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Oligocene|Oligocene|Mory (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Comprises claystones, marls and calcisiltites.||||||01-MAR-10
3707|Cartier Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Neogene|Browse Basin.||||Overlies Grebe and Prion Formations. Is overlain by Oliver Formation.||
3707|Cartier Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60, p410|Oligocene|Eocene|Up to 290m thick; restricted to outer part of Bonaparte Basin.||||Overlies Hibernia Formation (disconformably).|Shale, minor marl and limestone.|
3707|Cartier Formation|13353|6|Mentioned|p401 Fig.2.|Neogene|Paleogene|||||Overlies Grebe and Prion Formations. Is overlain by Oliver Formation.||
3707|Cartier Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Neogene|Unit of Woodbine Group. Overlies Grebe and Prion Formations and underlies Oliver Formation.||91||||28-OCT-14
3707|Cartier Formation|24218|5|Briefly described|p850|Oligocene|Oligocene|Geological Province: Bonaparte Basin.||||||
3707|Cartier Formation|41437|6|Mentioned|Fig.3|||||||||
3707|Cartier Formation|41532|4|Described|p309|||||||||
3707|Cartier Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
3707|Cartier Formation|42442|3|Fully described|p31|Aquitanian|Oligocene|Age Oligocene to earliest Miocene (Aquitanian).||||||14-APR-08
3707|Cartier Formation|43699|6|Mentioned|Fig.6,p10|Miocene|Oligocene|||||||
3707|Cartier Formation|49637|5|Briefly described|Fig. 3|Miocene|Oligocene|Geological Province: Ashmore Platform.||||||07-FEB-11
3707|Cartier Formation|61548|6|Mentioned|p480 Fig.3|Oligocene|Oligocene|Northern Bonaparte Basin.||||||
3707|Cartier Formation|62837|5|Briefly described|Stratigraphic columns|Oligocene|Oligocene|Age: ~30Ma. Geological Province: Ashmore Platform and Northern Bonaparte Basin.||||||01-MAR-10
3707|Cartier Formation|63358|5|Briefly described|p4 Fig. 1.3|Miocene|Oligocene|||||||01-MAR-10
3707|Cartier Formation|64695|5|Briefly described|p262 |Late Oligocene|Late Oligocene|Occurs to the N and NW of the Fohn-1 region; not in this study area.||||Overlies Prion Formation. Is overlain by Oliver Formation.||
3707|Cartier Formation|65680|6|Mentioned|p709 Fig.2.|Chattian|Chattian|||||Unconformably overlies Hibernia Formation. Is overlain by Oliver Formation.||
3707|Cartier Formation|66187|5|Briefly described|p423|Oligocene|Oligocene|||||||
3707|Cartier Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Oligocene|Oligocene|||||||
3707|Cartier Formation|69297|5|Briefly described|p305|Aquitanian|Chattian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlain by the Oliver Formation.||
3707|Cartier Formation|69452|5|Briefly described|p36:15|Neogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
3707|Cartier Formation|70061|5|Briefly described|Regional geology; Figs.6-7. Sahul: Fig.2|Miocene|Oligocene|See also Vulcan: p3. Hydrocarbon reservoir in Vulcan Sub-basin.||Woodbine Group.||Overlies Prion Formation. Is overlain by Oliver Formation. Equivalent to Oliver Sandstone Member.||12-JUL-16
3707|Cartier Formation|70064|5|Briefly described|Regional Fig. 6. Central Fig.2|Miocene|Oligocene|See also Northern: Fig.2. Yampi: Fig.2. Brecknoff-Scott Reef Trend and Prudhoe Terrace, Browse Basin.||Woodbine Group.||Is overlain by Oliver Sandstone Member or Oliver Formation.||12-JUL-16
3723|Carynginia Formation|5257|6|Mentioned|p153|Permian|Permian|Perth Basin. Core from Woodada 3 and Beekeeper 1 formerly included in this Formation is now considered younger than type Carynginia Fm, so is now included in the Beekeeper Member, Wagina Fm.||||||04-MAY-11
3723|Carynginia Formation|12758|5|Briefly described|p8 Fig. 9|Permian|Permian|Geological Province: Northern Perth Basin.||||||21-JUL-09
3723|Carynginia Formation|14227|5|Briefly described|p7|Kungurian|Artinskian|Marine muds and sands. Contains gas prone source rocks. See also Enclosure 2.||||||07-FEB-11
3723|Carynginia Formation|14228|6|Mentioned|p5 fig 2|Early Permian|Early Permian|||||Overlies Irwin River Coal Measures.||
3723|Carynginia Formation|22814|5|Briefly described|fig2|Permian|Permian|||||||
3723|Carynginia Formation|22820|5|Briefly described|p10 Fig.4, p21|Late Permian|Early Permian|Geological province: northern Perth Basin. Correlates with Redgate C.M.||||||12-AUG-08
3723|Carynginia Formation|23172|4|Described|Map Legend|Permian|Permian|||||||
3723|Carynginia Formation|23174|3|Fully described|p5-6,14|Early Permian|Early Permian|||||||
3723|Carynginia Formation|23279|4|Described|p14-6||Artinskian|||||||
3723|Carynginia Formation|23520|5|Briefly described|p6 Fig. 4|Early Permian|Early Permian|Geological Province: Abrolhos Sub-basin. See also p18.||||||21-JUL-09
3723|Carynginia Formation|23726|6|Mentioned|p47|||Geological Province: Perth Basin.||||||
3723|Carynginia Formation|23761|5|Briefly described|p11|||Mainly siltstone and shale with small interbedded sandstone.||||||
3723|Carynginia Formation|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||23-DEC-09
3723|Carynginia Formation|23816|4|Described|p234|Kungurian|Artinskian|Formerly known as "Carynginia Shale". Geological Province: Perth Basin. Overlying unit: Wagina Sandstone (unconformable). Underlying unit: Irwin River Coal Measures (conformable). Max. thickness: 349 m. Fossiliferous.||||||
3723|Carynginia Formation|24058|6|Mentioned|p117|||||||||
3723|Carynginia Formation|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
3723|Carynginia Formation|24351|5|Briefly described|Plate 3 (in pocket)|Middle permian|Middle permian|Log Wittecarra-1.||||||13-DEC-07
3723|Carynginia Formation|24390|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin.||||||
3723|Carynginia Formation|24443|5|Briefly described|Fig.30|Early Permian|Early Permian|Conformably overlies Irwin River Coal Measures. Unconformably overlain by Beekeeper Formation (and equivalent), Dongara Sandstone and Wagina Sandstone. Geological Province: Bight Basin.||||||21-JUL-09
3723|Carynginia Formation|29721|6|Mentioned|p226|||||||||
3723|Carynginia Formation|29790|6|Mentioned|p91|||||||||
3723|Carynginia Formation|30545|6|Mentioned|Fig.2|||Artinskian||||||
3723|Carynginia Formation|30565|6|Mentioned|p116|||||||||
3723|Carynginia Formation|30973|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
3723|Carynginia Formation|31394|6|Mentioned|p60|||See also P61,62.L.Permian||||||
3723|Carynginia Formation|31561|5|Briefly described|p18|||See also P20. Map.||||||
3723|Carynginia Formation|31562|6|Mentioned|Fig. 3|||||||||
3723|Carynginia Formation|31568|5|Briefly described|p19|||L. Permian||||||
3723|Carynginia Formation|31910|4|Described|p17|||Table 1||||||
3723|Carynginia Formation|32165|6|Mentioned|p196|||Sections correlated BMR10 & 10A||||||
3723|Carynginia Formation|32337|4|Described|p25|||||||||
3723|Carynginia Formation|32641|6|Mentioned|p5|||||||||
3723|Carynginia Formation|32648|6|Mentioned|p32|||L.Perm.||||||
3723|Carynginia Formation|32649|4|Described|p22|||||||||
3723|Carynginia Formation|32714|6|Mentioned|Fig.2|||||||||
3723|Carynginia Formation|32840|6|Mentioned|Table 1|||||||||
3723|Carynginia Formation|32979|6|Mentioned|p38|||Correlation with basins in India||||||
3723|Carynginia Formation|33022|5|Briefly described|p263|||Palaeomagnetism. See also P261.||||||
3723|Carynginia Formation|33052|6|Mentioned|p515|||See also Fig.1. Artinskian & Kungurian||||||
3723|Carynginia Formation|33386|6|Mentioned|Fig.7|||||||||
3723|Carynginia Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
3723|Carynginia Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
3723|Carynginia Formation|34274|6|Mentioned|p118|||Perm. See also Fig.2||||||
3723|Carynginia Formation|34532|6|Mentioned|Fig.2|||||||||
3723|Carynginia Formation|34841|6|Mentioned|p95|||||||||
3723|Carynginia Formation|35282|6|Mentioned|Fig.2|||||||||
3723|Carynginia Formation|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
3723|Carynginia Formation|36100|6|Mentioned|Fig.2|||||||||
3723|Carynginia Formation|36257|6|Mentioned|Table 2.1|||||||||
3723|Carynginia Formation|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
3723|Carynginia Formation|36266|6|Mentioned|p150|||||||||
3723|Carynginia Formation|36293|2|Defined|p106|Artinskian|Artinskian|||||||
3723|Carynginia Formation|36890|3|Fully described|p234|||Formerly Carynginia Shale.||||||11-APR-08
3723|Carynginia Formation|36899|6|Mentioned|p1091|||||||||
3723|Carynginia Formation|36911|6|Mentioned|p57|||||||||
3723|Carynginia Formation|37104|6|Mentioned|Fig.3|||||||||
3723|Carynginia Formation|37286|6|Mentioned|p30|||||||||
3723|Carynginia Formation|37298|6|Mentioned|Fig.1|||||||||
3723|Carynginia Formation|37340|6|Mentioned|p170|||||||||
3723|Carynginia Formation|37577|6|Mentioned|p77|||||||||
3723|Carynginia Formation|37703|6|Mentioned|p2243|||||||||
3723|Carynginia Formation|37812|6|Mentioned|p653|||||||||
3723|Carynginia Formation|38484|6|Mentioned|p6|||||||||
3723|Carynginia Formation|38486|6|Mentioned|p6|||||||||
3723|Carynginia Formation|38655|6|Mentioned|p6|||||||||
3723|Carynginia Formation|38732|6|Mentioned|p31|||||||||
3723|Carynginia Formation|38772|6|Mentioned|p50|||||||||
3723|Carynginia Formation|39316|6|Mentioned|p328|||||||||
3723|Carynginia Formation|39757|6|Mentioned|p1605|||||||||
3723|Carynginia Formation|39854|6|Mentioned|p21|||||||||
3723|Carynginia Formation|40306|6|Mentioned|p59|||||||||
3723|Carynginia Formation|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
3723|Carynginia Formation|40347|5|Briefly described|p25|||||||||
3723|Carynginia Formation|40992|6|Mentioned|p6|||Mention Fig.5||||||
3723|Carynginia Formation|41172|4|Described|p123|||||||||
3723|Carynginia Formation|41192|6|Mentioned|p290|||||||||
3723|Carynginia Formation|41195|6|Mentioned|p321|||||||||
3723|Carynginia Formation|41284|6|Mentioned|p89|||||||||
3723|Carynginia Formation|41589|6|Mentioned|p118|||||||||
3723|Carynginia Formation|41728|6|Mentioned|p441|||||||||
3723|Carynginia Formation|41729|6|Mentioned|p453|||||||||
3723|Carynginia Formation|42075|5|Briefly described|Fig.7 P247|||||||||
3723|Carynginia Formation|43015|5|Briefly described|Table 1,p319|||||||||
3723|Carynginia Formation|43018|5|Briefly described|Table 1,p386|||||||||
3723|Carynginia Formation|43031|5|Briefly described|Fig,2.p12.|||||||||
3723|Carynginia Formation|43050|5|Briefly described|p6|||||||||
3723|Carynginia Formation|43067|5|Briefly described|p120,Fig.12,p124|||||||||
3723|Carynginia Formation|43216|5|Briefly described|Map Legend||Permian|Perth Basin||||||
3723|Carynginia Formation|43217|5|Briefly described|Map Legend||Permian|Perth Basin||||||
3723|Carynginia Formation|43296|6|Mentioned|Map Legend||Permian|||||||
3723|Carynginia Formation|43297|4|Described|p4, fig.3 p5||Artinskian|Type section location given. Also Table1 p7.||||||
3723|Carynginia Formation|43347|6|Mentioned|13|||||||||
3723|Carynginia Formation|43495|4|Described|6-32||Artinskian|||||||
3723|Carynginia Formation|43504|4|Described|4-17|Kungurian|Artinskian|||||||
3723|Carynginia Formation|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p510-512|Artinskian|Artinskian|See also p515, p523. Type area Carynginia Gully (no type section). Reference Section Woolaga Creek 29o11'20''S 115o39'30''E. Up to 350m thick shallow marine sediments. Unnamed limestone member in Woodada area. Mis-spelt as Caryinginia Formation in Fig.4-145. A limestone (shelly-carbonate sand) member in this unit is the reservoir in the Woodada Gasfield.||||Conformably overlies Irwin River Coal Measures. Overlain by Wagina Sandstone (disconformably).|Black, grey, brown or yellow micaceous siltstone and quartz sandstone; minor fine conglomerate; limestone.|
3723|Carynginia Formation|44219|14|Not recorded|p31||Artinskian|||||||
3723|Carynginia Formation|44237|14|Not recorded|p.201, 203|||Fig.2.||||||
3723|Carynginia Formation|44994|6|Mentioned|Fig.7|||Correlation||||||
3723|Carynginia Formation|45001|4|Described|p145-146|||Compared with Keogh Formation.||||||25-NOV-16
3723|Carynginia Formation|46849|6|Mentioned|p186|||||||||
3723|Carynginia Formation|47041|6|Mentioned|p166|||||||||
3723|Carynginia Formation|48614|14|Not recorded|p46,47, Pl.8|||||||||
3723|Carynginia Formation|48615|4|Described|p.3,4,5.|||(H50-9)||||||
3723|Carynginia Formation|48857|2|Defined|p.11,15-17|||||||||
3723|Carynginia Formation|49644|5|Briefly described|Table|||||||||
3723|Carynginia Formation|49942|5|Briefly described|p4 Fig.3|Early Permian|Early Permian|Conformably overlies Irwin River Coal Measures. Geological Province: Gascoyne Platform.||||||
3723|Carynginia Formation|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
3723|Carynginia Formation|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
3723|Carynginia Formation|60377|4|Described|p61 Fig. 3, p63, p72|Roadian|Artinskian|Underlain by Irwin River Coal Measures. Geological Province: Perth Basin. Depositional Environment is marine. Consists of fine-grained siltstones that are highly carbonaceous and often micaceous.||||||07-FEB-11
3723|Carynginia Formation|60384|6|Mentioned|p243, Fig 2a||Early Permian|Perth Basin.||||||
3723|Carynginia Formation|60386|5|Briefly described|p304, 311|||Perth Basin. Marine. See also mis-spelling Carrynginia Fm p297.||||Overlain by Wagina Formation and Dongara Sandstone.||
3723|Carynginia Formation|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||11-APR-08
3723|Carynginia Formation|61546|6|Mentioned|p385 Fig.5.|Early Permian|Early Permian|||||Overlies Irwin River Coal Measures.||
3723|Carynginia Formation|61811|4|Described|p3 Fig.2, p36, pp39-45, p62.|Kungurian|Artinskian|Northern Perth Basin. Formerly Carynginia Shale (Clarke et al. 1951); amended to Formation status by Playford and Willmott, in McWhae et al. (1958). Restricted marine facies. Type section in Carynginia Gully, a tributary of North Branch of the Irwin River; further details in Appendix 1. Similar facies to Holmwood Shale.||||Overlies Irwin River Coal Measures. Is overlain unconformably by Wagina Sandstone.|Black to grey micaceous jarositic shale and siltstone, with lesser interbedded sandstone and conglomerate; ice-rafted erratic pebbles and boulders of granite and metamorphic rocks common.|
3723|Carynginia Formation|62113|4|Described|pp618-621, p627 Fig.10, pp629-630.|Roadian|Artinskian|Up to 300m of fine-grained, siliciclastic deposits, reflecting mid-shelf setting during renewed basin subsidence. Palynomorphs are mostly from the Kungurian p.sinuous zone (Backhouse 1993). The carbonaceous shales are a potential hydrocarbon source rock.||||Overlies the Irwin River Coal Measures.|Transgressive shale with ice-rafted, commonly outsize clasts to 1.8 m diameter of granite and gneiss; deeper-water, laminated, bioturbated and deformed mudstones with lenticular beds of symmetrically-rippled and swaly cross-stratified sandstone.|
3723|Carynginia Formation|64580|4|Described|map legend||Early Permian|Micaceous siltstone and quartz sandstone, minor granule to pebble conglomerate, limestone.||||||09-DEC-08
3723|Carynginia Formation|64630|5|Briefly described|p31 Fig.2, p34|Kungurian|Artinskian|Province: Northern Perth Basin. Overlies the Irwin River Coal Measures. Palynology age: M trisina to P. sinuosis.||||||24-NOV-09
3723|Carynginia Formation|64635|5|Briefly described|p4 Fig.3, p18, p20-26     |Kungurian|Artinskian|Formerly the Carynginia Shale (Clarke et al., 1951). Renamed by Playford and Willmott, in McWhae et al., (1958). Restricted marine facies. Type section diagram p22 Fig.20. Artinskian-Kungurian age based on palynomorph assemblages (Segroves 1971; Backhouse 1993).||||Lower part appears to be laterally equivalent to the Mingenew Formation. Overlies the Irwin River Coal Measures. Conformably or disconformably overlain by the Wagina Sandstone.|Black to grey micaceous jarositic shale and siltstone with lesser interbedded sandstone and conglomerate; erratic (probably ice-rafted) pebbles and boulders of granite and metamorphic rocks are common; extensive bioturbation.|
3723|Carynginia Formation|64972|6|Mentioned|p617 Fig. 5|Permian|Permian|Geological Province: Perth Basin.||||||
3723|Carynginia Formation|64974|6|Mentioned|p144 Fig. 3|Kungurian|Artinskian|Geological Province: Perth Basin.||||||24-JUN-09
3723|Carynginia Formation|64980|5|Briefly described|pp625-634.|Permian|Permian|Perth Basin. Hydrocarbon reservoir and gas source.||||Overlies Irwin River Coal Measures.|Shallow marine, carbonaceous siltstone and shale, with interbedded 1 to 4 m thick regular beds of sandstone..|
3723|Carynginia Formation|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin.||||Overlies Irwin River and Sue Coal Measures.|Shale, mudstone.|
3723|Carynginia Formation|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
3723|Carynginia Formation|67370|5|Briefly described|p323 Fig.14, pp327-328.|Kungurian|Artinskian|Perth Basin. Alpine glacial episodes.|||||Thick transgressive shales containing ice-rafted debris.|
3723|Carynginia Formation|67925|5|Briefly described|Ch4 p8 fig 2|Upper Permian|Lower Permian|Northern and central Perth Basin. ||||Overlies the Irwin River Coal Measures. Unconformably overlain by the Wagina Sandstone.||
3723|Carynginia Formation|67977|5|Briefly described|p479|Kungurian|Artinskian|Geol. Prov: northern Perth Basin||||||
3723|Carynginia Formation|69029|6|Mentioned|p313,315,330,332-333|Wordian|Roadian|Of Canning Basin, Perth Basin. Main oil-prone source beds in Perth Basin with TOC of >2%. May host roughly half of estimated total shale-gas resources for the Perth Basin (Kuuskraa et al., 2011).||||Overlain by Willespie Formation. Underlain by Ashbrook Sandstone.||
3723|Carynginia Formation|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p11, Ch2 p44-p49|Late Permian|Late Permian|Perth Basin. Forms a regional seal along with the Kockatea Shale. See also  Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p72, Ch2 p80, Ch2 p84,Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98-p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110. ||||Overlies the Irwin River Coal Measures. Unconformably overlain by the Beekeeper Formation and conformably overlain by the Wagina Sandstone. Grades laterally into the Sue Group.|Bioturbated sandy claystone containing shallow-marine reservoir sandstones.|
3723|Carynginia Formation|69297|6|Mentioned|p237|||||||||
3723|Carynginia Formation|69547|5|Briefly described|p182,193,201|Kungurian|Artinskian|northern Perth Basin. Characterised by siliciclastic facies with prominent mud-sand cyclicity in lower part of the section.  Dropstones in the basal part of the section indicate glaciation.||||||
3723|Carynginia Formation|70097|5|Briefly described|p2, p10, p20 Fig.4|Artinskian||Northern Perth Basin. Irwin Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies Irwin River Coal Measures. Is overlain by Beekeeper Formation, Wagina or Dongara Sandstones.|Marine sediments.|30-SEP-16
3723|Carynginia Formation|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Irwin River Coal Measures. Is overlain conformably by Beekeeper Formation.||
3723|Carynginia Formation|70774|5|Briefly described|p5 fig 3|Kungurian|Artinskian|Northern Perth Basin.||||Overlies the Irwin River Coal Measures.||
3723|Carynginia Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Roadian|Artinskian|Perth Basin. Formed during Gondwana breakup along the western margin.|290.1  268.8 Ma (biostrat)||||Micaceous siltstone and quartz sandstone, minor granule to pebble conglomerate, limestone|
3723|Carynginia Formation|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Perth Basin.||||||
3723|Carynginia Formation|71146|5|Briefly described|p6, p36, p38,  p43 fig 33, p44|Kungurian|Artinskian|Perth Basin.||||Overlies the Irwin River Coal Measures. Overlain by the Beekeeper Formation.|Mudstone.|
3723|Carynginia Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, sandstone, conglomerate, siltstone|
3723|Carynginia Formation|71269|4|Described|GEOL_LUT_CSV files|Kungurian|Artinskian|Of Perth Basin. Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma)??. See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|201.3-166.1 Ma (biostrat)||||Micaceous siltstone and quartz sandstone, minor granule to pebble conglomerate, limestone|
3723|Carynginia Formation|71623|5|Briefly described|p348, p345 fig 2, p349 fig 7, p350, p354|Kungurian|Kungurian|Perth Basin. ||||Unconformably overlain by Beekeeper Formation.|Shale|
3723|Carynginia Formation|72034|5|Briefly described|500k_interpgeop16_lut|Kungurian|Artinskian|Perth Basin.  Age from biostratigraphy.||Permian package 2, Perth Basin.|||Micaceous siltstone and quartz sandstone, minor granule to pebble conglomerate, limestone.|
3723|Carynginia Formation|72258|5|Briefly described|p129|Guadalupian|Cisuralian|Of Perth Basin.||||Overlain by Beekeeper Formation. Underlain by Carynginia Formation.||
3723|Carynginia Formation|72505|5|Briefly described|p890|Roadian|Kungurian|Perth Basin. Correlated with Microbaculispora trisina, P.sinuosus, praecolpatites sinuosis and Microbaculispora villosa zones.||||Overlies the Irwin River Coal Measures.||
3723|Carynginia Formation|72910|5|Briefly described|p4 Fig.3, p31 App. 2|Late Permian|Early Permian|Shown as part of the Northern Perth Basin. Recognised in Candace 1 well and processed for palynology (moderate yield).  Assigned to ?P. pseudoreticulata zone.||||||
3723|Carynginia Formation|73117|6|Mentioned|p15|Kungurian|Artinskian|||||Correlates to Byro Group.||
3723|Carynginia Formation|73184|6|Mentioned|p199|Kungurian|Kungurian|Perth Basin.|||||Mudstones with ice-rafted debris and cold-water fauna.|
3723|Carynginia Formation|73484|6|Mentioned|p476 Fig.3|Cisuralian|Cisuralian|Perth Basin. Marine clays and silts.||||Overlies Irwin River Coal Measures||
3723|Carynginia Formation|73513|4|Described|p29, p30 Fig.2, p32-33, p39-41|Kungurian|Artinskian|Perth Basin. Marine shelfal conditions. Acts as a major regional seal. About 150 m thick in the Waitsia area.||||Overlies Irwin River Coal Measures, underlies Wagina Sandstone|Marine rocks, shale dominated.|
3723|Carynginia Formation|73623|5|Briefly described|p4|Cisuralian|Cisuralian|Irwin Basin.||||Overlies Irwin River Coal Measures. Is overlain by Wagina Sandstone. Correlative of Byro Group.||
3734|Cashin Member|40617|6|Mentioned|p14|||||||||
3734|Cashin Member|41271|4|Described|p166|||||||||
3734|Cashin Member|61155|5|Briefly described|p15|Early Eocene|Early Eocene|Of the Cardabia Calcarenite. Age: ~56Ma. Geological Province: Carnarvon Basin/onshore.||||||03-MAR-10
3764|Castlereagh Hill Porphyry|22547|3|Fully described|p10|Orosirian|Orosirian|Age: 1865- 1850 Ma. Part of the Whitewater Volcanics reassigned to Castlereagh Hill Porphyry. Porphyric rock unit of Castlereagh Hill redefined as Greenvale Porphyry.||||||06-AUG-08
3764|Castlereagh Hill Porphyry|22754|5|Briefly described|p6|||||||||
3764|Castlereagh Hill Porphyry|23751|4|Described|p8|Proterozoic|Proterozoic|||||||
3764|Castlereagh Hill Porphyry|24197|5|Briefly described|p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
3764|Castlereagh Hill Porphyry|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
3764|Castlereagh Hill Porphyry|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
3764|Castlereagh Hill Porphyry|32660|5|Briefly described|Table 1|||||||||
3764|Castlereagh Hill Porphyry|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
3764|Castlereagh Hill Porphyry|32728|5|Briefly described|p29|||See also Fig.3||||||
3764|Castlereagh Hill Porphyry|36885|4|Described|p171|||||||||
3764|Castlereagh Hill Porphyry|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
3764|Castlereagh Hill Porphyry|39889|6|Mentioned|p495|||||||||
3764|Castlereagh Hill Porphyry|41158|6|Mentioned|p36|||||||||
3764|Castlereagh Hill Porphyry|41961|6|Mentioned|Table 1 P39|||||||||
3764|Castlereagh Hill Porphyry|41977|5|Briefly described|p472|||||||||
3764|Castlereagh Hill Porphyry|43853|5|Briefly described|Map Legend||Proterozoic|||||||
3764|Castlereagh Hill Porphyry|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
3764|Castlereagh Hill Porphyry|44155|4|Described|p234 Tb.3-2, p240-241, p243 Tb.3-6|Paleoproterozoic|Paleoproterozoic|See also p248 Tb.3-8. East Kimberley. Comagmatic with Whitewater Volcanics; Bickleys and Mount Disaster Porphyries.||Lamboo Complex||Intrudes and intruded by Bow River Granite. Intrudes or unconformably overlies Halls Creek Group.|Grey quartz-feldspar porphyry and monzogranite.|
3764|Castlereagh Hill Porphyry|44230|5|Briefly described|Map Legend||Proterozoic|||||||
3764|Castlereagh Hill Porphyry|44317|14|Not recorded|Table 1||Proterozoic|||||||
3764|Castlereagh Hill Porphyry|44318|14|Not recorded|map legend||Proterozoic|Proterozoic.||||||
3764|Castlereagh Hill Porphyry|44363|5|Briefly described|p.7,8,9,12,17,29||Paleoproterozoic|Lower Proterozoic, Lamboo Complex.||||||07-NOV-08
3764|Castlereagh Hill Porphyry|44364|14|Not recorded|map legend|||||||||
3764|Castlereagh Hill Porphyry|44868|5|Briefly described|Map Legend||Proterozoic|||||||
3764|Castlereagh Hill Porphyry|45047|4|Described|p13|||See also p26.||||||03-AUG-06
3764|Castlereagh Hill Porphyry|45048|3|Fully described|p63|||Carpentarian or Lower Proterozoic||||||
3764|Castlereagh Hill Porphyry|45050|6|Mentioned|p7|||||||||
3764|Castlereagh Hill Porphyry|46797|6|Mentioned|p81|||Dates||||||
3764|Castlereagh Hill Porphyry|48938|6|Mentioned|p9|||Correlation.||||||
3764|Castlereagh Hill Porphyry|50437|5|Briefly described|p1.6, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite. Age: 1855 +/- 2Ma (Shrimp).||||||07-NOV-08
3764|Castlereagh Hill Porphyry|63866|5|Briefly described|p132|||Co-magmatic with the Whitewater Volcanics and the Greenvale Porphyry.||||||
3764|Castlereagh Hill Porphyry|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|In Hooper Complex and Western Zone of Hall Creek Orogen.|1860 - 1850 Ma.|||Co-magmatic with Whitewater Volcanics.||12-APR-12
3764|Castlereagh Hill Porphyry|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This magmatic crystallisation age is based on 20 data points.|1855+/-4 Ma U/Pb SHRIMP|Paperbark Supersuite|||Porphyritic microgranodiorite; fine- and medium-grained phenocrysts of plagioclase and K-feldspar.|30-JUL-15
3764|Castlereagh Hill Porphyry|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1855 Ma|Paperbark Supersuite|||Porphyritic microgranodiorite; fine- and medium-grained phenocrysts of plagioclase and K-feldspar.|
3764|Castlereagh Hill Porphyry|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1864-1854 Ma (Inferred)|Unit of Paperbark Supersuite.|||Porphyritic microgranodiorite; fine- and medium-grained phenocrysts of plagioclase and K-feldspar|
3764|Castlereagh Hill Porphyry|70154|6|Mentioned|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv.|1854-1864 Ma|Paperbark Supersuite||||
3764|Castlereagh Hill Porphyry|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1864-1854 Ma (inferred)|Unit of Paperbark Supersuite.|||Quartz-feldspar porphyry, hornblende-biotite granodiorite, porphyritic microgranodiorite; fine- and medium-grained phenocrysts of plagioclase and K-feldspar|
3764|Castlereagh Hill Porphyry|72437|5|Briefly described|p5, p39|||Lamboo Complex. Co-magmatic with the Whitewater Volcanics.|||||Microgranite.|
3806|Cattamarra Coal Measures|12758|5|Briefly described|p17, p3 Fig. 3|Early Jurassic|Early Jurassic|Conformably overlain by Cadda Formation and Yarragadee Formation; overlies the Eneabba Formation conformably, and Lesueur Sandstone. Geological Province: Perth Basin. See also p8 Fig. 9.||||||01-OCT-08
3806|Cattamarra Coal Measures|12759|3|Fully described|p27; p28 Tb. 7; p173 Pl. 1|Pliensbachian|Aalenian|Formerly Cattamarra Coal Measures Member; given Formation status (Mory 1994); replaces Cockleshell Gully Formation (Playford and Low, 1972) in Perth Region. Type section in Eneabba No. 1 Well. >500 m thick.||||Conformably underlies Yarragadee Formation.||12-MAY-14
3806|Cattamarra Coal Measures|14227|5|Briefly described|p8, p10|Jurtassic|Jurassic|Overlies Eneabba Formation; underlies Cadda Formation. Coal-bearing, delta-top sandstones. See also Enclosure 2.||||||07-FEB-11
3806|Cattamarra Coal Measures|22814|5|Briefly described|p254, fig2|Jurassic|Jurassic|||||||
3806|Cattamarra Coal Measures|23172|4|Described|Map Legend|Jurassic|Jurassic|||||||
3806|Cattamarra Coal Measures|23279|3|Fully described|p2,26-7|Aalenian|Pliensbachian|||||||
3806|Cattamarra Coal Measures|23520|5|Briefly described|p6 Fig. 4|Middle Jurassic|Early Jurassic|Underlies and is sealed by the Cadda Formation. See also p9 and p32.||||||21-JUL-09
3806|Cattamarra Coal Measures|23578|5|Briefly described|p6|Jurassic|Jurassic|See also p13 Tb. 1||||||
3806|Cattamarra Coal Measures|23579|5|Briefly described|Map Legend|||||||||
3806|Cattamarra Coal Measures|24374|5|Briefly described|p8|||Geological Province: Perth Basin.||||||
3806|Cattamarra Coal Measures|24375|5|Briefly described|p9|Jurassic|Jurassic|Geological Province: Dandaragan Trough, Perth Basin||||||24-FEB-05
3806|Cattamarra Coal Measures|24390|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
3806|Cattamarra Coal Measures|24430|5|Briefly described|p39|Jurassic|Jurassic|Geological Province: Dandaragan Trough||||||03-MAR-05
3806|Cattamarra Coal Measures|24443|5|Briefly described|p31, Fig.39|Middle Jurassic|Early Jurassic|Overlies Eneabba Formation. Overlain by Cadda Formation. Geological Province: Houtman Sub-basin.||||||21-JUL-09
3806|Cattamarra Coal Measures|31649|6|Mentioned|p63|||Supersedes Cattamarra Coal Measures Member.||||||
3806|Cattamarra Coal Measures|33166|6|Mentioned|Table 1|||Correlation chart||||||
3806|Cattamarra Coal Measures|34841|6|Mentioned|p98|||||||||
3806|Cattamarra Coal Measures|35573|6|Mentioned|p35|||||||||
3806|Cattamarra Coal Measures|35653|6|Mentioned|p1094|||Discussion of stratigraphy and basin development.||||||
3806|Cattamarra Coal Measures|36100|6|Mentioned|Fig.2|||||||||
3806|Cattamarra Coal Measures|36265|5|Briefly described|p134|Early Jurassic|Early Jurassic|Geological province: Perth Basin.||||||04-MAR-08
3806|Cattamarra Coal Measures|37114|6|Mentioned|p308|||||||||
3806|Cattamarra Coal Measures|37124|4|Described|p339|||||||||
3806|Cattamarra Coal Measures|38479|6|Mentioned|p15|||||||||
3806|Cattamarra Coal Measures|38486|6|Mentioned|p6|||||||||
3806|Cattamarra Coal Measures|38777|6|Mentioned|p29|||||||||
3806|Cattamarra Coal Measures|40305|4|Described|p76|||||||||
3806|Cattamarra Coal Measures|40358|6|Mentioned|p22|||||||||
3806|Cattamarra Coal Measures|40359|5|Briefly described|p22|||||||||
3806|Cattamarra Coal Measures|41172|5|Briefly described|p126|||||||||
3806|Cattamarra Coal Measures|41729|5|Briefly described|p454|||||||||
3806|Cattamarra Coal Measures|42150|6|Mentioned|p69|||||||||
3806|Cattamarra Coal Measures|43096|5|Briefly described|p38|||||||||
3806|Cattamarra Coal Measures|43197|5|Briefly described|Map Legend||Jurassic|||||||
3806|Cattamarra Coal Measures|43216|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
3806|Cattamarra Coal Measures|43217|5|Briefly described|Map Legend||Jurassic|Perth Basin||||||
3806|Cattamarra Coal Measures|43296|5|Briefly described|Map Legend||Jurassic|||||||
3806|Cattamarra Coal Measures|43297|3|Fully described|Fig.3p5,p12.Table1p6|Aalenian|Toarcian|Type section location given. Originally Cattamarra Coal Member. Age wrongly given as Triassic on p13.||||||14-NOV-07
3806|Cattamarra Coal Measures|43347|4|Described|5|Middle Jurassic|Early Jurassic|||||||
3806|Cattamarra Coal Measures|43495|4|Described|6-36|Aalenian||||||||
3806|Cattamarra Coal Measures|43504|4|Described|4-10|Middle Jurassic|Pliensbachian|||||||
3806|Cattamarra Coal Measures|44237|14|Not recorded|p.202|||Of Cockleshell Gully Formation.||||||
3806|Cattamarra Coal Measures|49942|5|Briefly described|p39|Jurassic|Jurassic|Geological Province: Abrolhos-Houtman Sub-basins. Probably an oil source rock.||||||
3806|Cattamarra Coal Measures|50085|5|Briefly described|p15 Fig. 8|Jurassic|Jurassic|Geological Province: Northern Perth Basin.||||||11-MAY-04
3806|Cattamarra Coal Measures|50107|5|Briefly described|Map legend|Jurassic|Jurassic|Geological Province: Perth Basin.||||||
3806|Cattamarra Coal Measures|60118|6|Mentioned|p29|||Geological Province: Perth Basin.||||||
3806|Cattamarra Coal Measures|60120|5|Briefly described|p36|Early Jurassic|Early Jurassic|Geological Province: northern Perth Basin.||||||22-JUL-04
3806|Cattamarra Coal Measures|60376|4|Described|p16, p26, p17 Fig. 4, p28.|Early Jurassic|Early Jurassic|Geological Province: Perth Basin. Overlain unconformably by Cadda Formation. Underlain by Eneabba Formation. Fine- to coarse-grained sandstones with dark carbonaceous siltstone and claystone interbeds, and coal seams up to 11m thick.||||||07-FEB-11
3806|Cattamarra Coal Measures|60384|6|Mentioned|p243 Fig 2a, p261|Middle Jurassic|Early Jurassic|Perth Basin. Source rocks|||||Includes coaly and carbonaceous facies.|
3806|Cattamarra Coal Measures|60386|6|Mentioned|p299|Middle Jurassic|Early Jurassic|Perth Basin. Non-marine.||||||
3806|Cattamarra Coal Measures|61023|5|Briefly described|p20 Fig 10|Jurassic|Jurassic|Geological Province: Perth Basin.||||||10-APR-08
3806|Cattamarra Coal Measures|61546|6|Mentioned|p383, p385 Fig.5. |Jurassic|Jurassic|||||||
3806|Cattamarra Coal Measures|61811|5|Briefly described|p3 Fig.2, p29, p48, p62.|Middle Jurassic|Early Jurassic|Northern Perth Basin. Is laterally equivalent to Chapman Group, further to the north. Type section details in Appendix 1.||||Overlies Eneabba Formation. Is overlain by Cadda Formation.||
3806|Cattamarra Coal Measures|64580|4|Described|map legend||Middle Jurassic|Carbonaceous siltstone, shale, claystone, coal, sandstone.||||||09-DEC-08
3806|Cattamarra Coal Measures|64635|5|Briefly described|p4 Fig.3, p16, p28   |Aalenian|Sinemurian|||||Overlies Eneabba Formation. Upper part is laterally equivalent to the upper Yarragadee Formation. Is overlain by Cadda Formation.||
3806|Cattamarra Coal Measures|67135|5|Briefly described|p5 Fig.7, p33 Fig.42.|Jurassic|Jurassic|Perth Basin.||||Overlies Eneabba Formation. Is overlain by Cadda Formation.||
3806|Cattamarra Coal Measures|67340|6|Mentioned|p6-8, 25, 50-63|Jurassic|Jurassic|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.||||||
3806|Cattamarra Coal Measures|67925|5|Briefly described|Ch2 p10 fig 4, Ch3 p8|Toarcian|Hettangian|Referred to as the obsolete Cattamarra Coal Measures Member on Ch4 p8 fig 2. See also Ch4 p8 fig 2, Ch4 p30 fig 34. ||||Overlies the Eneabba Formation. Overlain by the Cadda Formation and the Yarragadee Formation.||
3806|Cattamarra Coal Measures|68254|6|Mentioned|p1036 Fig.2, p1037 Tb.2, p1040, p1043|Jurassic|Jurassic|||||||
3806|Cattamarra Coal Measures|68811|6|Mentioned|p90, p180 tbl 39|Jurassic|Jurassic|||||||
3806|Cattamarra Coal Measures|69029|5|Briefly described|p330, p332|Aalenian|Pliensbachian|Of Perth Basin. In the Transitional petroleum system, the main oil- and gas-prone source beds are inside the fluvial-lacustrine shale facies in the Jurassic Cattamarra Coal Measures with TOC up to 27%.||||Overlain by Cada Formation. Underlain by Enneabba Formation.||04-SEP-19
3806|Cattamarra Coal Measures|69081|5|Briefly described|p735-8,p740-1, Figs.1 and 4, Tbs.1-3|Early Jurassic|Early Jurassic|Presented as Cattamarra C.M. in figure, and Cattamarra in table. Oil and gas produced. Lowest porosities with mean values around 5% of the four wells analysed. Geol. Prov: Perth Basin. See misspelt Cattamara Coal Measures.||||is overlain by Cadda Formation; overlies Eneabba Formation and Lesueur Sandstone|includes sandstones|
3806|Cattamarra Coal Measures|69182|5|Briefly described|p7, Ch2 p3, ch2 p14, Ch2 p20-p29|Middle Jurassic|Early Jurassic|Perth Basin. Misspelt as the Cattamara Coal measures on p7 and Ch2 p38. Generally has good porosity (over 10 percent) but poor permeability. Deposited in a swampy river environment. Good reservoir unit that is sealed by the Cadda Formation. See also Ch2 p34-p41, Ch2 p44-p46, Ch2 p52-p55, Ch2 p57, Ch2 p60-p63, Ch2 p67, Ch2 p69-p74, ch2 p76, Ch2 p79, Ch2 p83-p86, Ch2 p89-p90, Ch2 p93, Ch2 p97-p98, Ch2 p100, Ch2 p103-p112.||||Overlies the Eneabba Formation and the Lesueur Sandstone. Overlain by the Yarragadee and Cadda Formations.|Fine to coarse-grained sandstone and interbedded carbonaceous shale and siltstone.|
3806|Cattamarra Coal Measures|69297|6|Mentioned|p175, p189, p190, p206|Aalenian|Toarcian|Vlaming Sub-basin, South Perth Basin. ||||Overlain by the Yarragadee Formation.||
3806|Cattamarra Coal Measures|70097|5|Briefly described|p2, p7, p19-22 Figs.3-6|Bajocian|Toarcian|Deposition of delta-top swamp deposits. Includes marine interval interpreted to be source of oil. Perth Basin. Greenough/Bookara Shelf, Dongara Saddle, Dandaragan Trough, Beermullah Trough, Mandurah Terrace and Bunbury Trough.||||Overlies Lesueur Sandstone or Eneabba Formation. Is overlain by Yarragadee or Cadda Formations.||30-SEP-16
3806|Cattamarra Coal Measures|70099|5|Briefly described|Fig.4; p5|Bajocian|Rhaetian|Southern Perth Basin. Correlated to seismic package Mentelle 1C.||||Overlies Lesueur Sandstone. Is overlain by Yarragadee Formation.||
3806|Cattamarra Coal Measures|70128|5|Briefly described|p449, p451, p454-455, p457, p459-465|Early Jurassic|Early Jurassic|Perth Basin. Formerly called the Cockleshell Gully Formation. Modelled thickness distribution histogram. Has minimal unconformities: has undergone no significant erosion. Thickness differences indicate locally heterogeneous subsidence.||||Conformably overlies Eneabba Formation and Lesueur Sandstone. Is overlain conformably by Cadda and Yarragadee Formations.||
3806|Cattamarra Coal Measures|70796|5|Briefly described|500k_interpgeop14_lut.csv|Middle Jurassic|Lower Jurassic|Perth Basin. Formed during Gondwana breakup along the western margin.|201.3  163.5 Ma (biostrat)||||Carbonaceous siltstone, shale, claystone, coal, sandstone.|
3806|Cattamarra Coal Measures|70826|6|Mentioned|p7 tbl 4|Jurassic|Jurassic|Perth Basin.||||||
3806|Cattamarra Coal Measures|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, coal, sandstone|
3806|Cattamarra Coal Measures|71269|5|Briefly described|500k_interpgeop16_lut.csv|Bathonian|Early Jurassic|Of Perth Basin. Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);|286-272.3 Ma (biostrat)||||Carbonaceous siltstone, shale, claystone, coal, sandstone|
3806|Cattamarra Coal Measures|71377|5|Briefly described|p3, p7, p17|Middle Jurassic|Early Jurassic|Perth Basin. Not intersected in GSWA Harvey 1.||||Conformably overlies the Eneabba Formation. Overlain by the Cadda Formation and the Yarragadee Formation.||
3806|Cattamarra Coal Measures|71958|5|Briefly described|p34|Early Jurassic|Early Jurassic|Vlaming Sub-basin.||||Overlies the Eneabba Formation and the Lesueur Sandstone. Overlain by the Cadda Formation and Yarragadee Formation.||
3806|Cattamarra Coal Measures|72034|5|Briefly described|500k_interpgeop16_lut|Bathonian|Early Jurassic|Perth Basin.  Age from biostratigraphy.|||||Carbonaceous siltstone, shale, claystone, coal, sandstone.|
3806|Cattamarra Coal Measures|72258|5|Briefly described|p129|Early Jurassic|Early Jurassic|Of Perth Basin.||||Overlain by Yarragadee Formation or Cadda Formation. Underlain by, and laterally grades northward to Eneabba Formation. Also underlain by Lesueur Sandstone.||
3806|Cattamarra Coal Measures|73513|5|Briefly described|p30 Fig.2, p33|Bajocian|Pliensbachian|Perth Basin.||||Overlies Eneabba Formation, underlies Cadda Formation|Fluvial unit.|
3816|Cattlin Creek pegmatite|34723|6|Mentioned|p236|||||||||
3816|Cattlin Creek pegmatite|50542|5|Briefly described|p121-122, p123|||Informal name. Hosted by Annabelle Volcanics. Geological Province: Yilgarn Craton.||||||07-FEB-11
3850|Cecil Sandstone|13194|4|Described|p393 Tb. 4-16|Frasnian|Frasnian|Type Section: near Kununurra 15o47'S 128o46'E. 110-300m thick fluvial deposits.||Cockatoo Group||Overlies Abney Sandstone and Ragged Range Conglomerate (both conformably). Overlain by Hargreaves Formation.|Quartz sandstone, pebbly sandstone, minor pebble conglomerate, and siltstone.|
3850|Cecil Sandstone|40993|6|Mentioned|p4|||||||||
3850|Cecil Sandstone|41598|6|Mentioned|p412|||||||||
3850|Cecil Sandstone|41864|3|Fully described|p53|||||||||
3850|Cecil Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
3850|Cecil Sandstone|42030|5|Briefly described|p749|||||||||
3850|Cecil Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
3850|Cecil Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
3850|Cecil Sandstone|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
3850|Cecil Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
3892|Challis Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 15|Late Triassic|Late Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
3892|Challis Formation|7142|6|Mentioned|p350 Fig.4.|Late Triassic|Late Triassic|Browse Basin.||||Overlies Pollard Formation. Is overlain by Nome Formation.||
3892|Challis Formation|13194|4|Described|p386 Tb. 4-16|Carnian|Ladinian|Type Section: Challis 1 well (1387-2184m). Up to 559m thick open marine shelf deposits.||Sahul Group||Overlies Pollard Formation (conformably). Interfingers with Benalla Formation.|Interbedded shale, sandstone and carbonate.|
3892|Challis Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
3892|Challis Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Late Triassic|Late Triassic|Bonaparte Basin. Unit of Sahul Group. Overlies Pollard Formation and underlies Malita Formation.||96||||28-OCT-14
3892|Challis Formation|22663|5|Briefly described|AC97 1-4 p3||Triassic|||||||01-MAR-10
3892|Challis Formation|23378|6|Mentioned|p180 Fig.2||Late Triassic|Of Sahul Group, Vulcan Sub-basin.||||||04-AUG-06
3892|Challis Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
3892|Challis Formation|24207|5|Briefly described|p209 Fig. 5|Late Triassic|Late Triassic|||||||01-MAR-10
3892|Challis Formation|41532|2|Defined|p302|Late Triassic|Middle Triassic|||||||
3892|Challis Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
3892|Challis Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
3892|Challis Formation|42150|6|Mentioned|p67|||||||||
3892|Challis Formation|42442|3|Fully described|p22|Carnian|Ladinian|Age: Middle to Late Triassic (Ladinian to Carnian). Variation of Challis Fm, WA.||||||
3892|Challis Formation|43711|6|Mentioned|p22|||||||||
3892|Challis Formation|43826|6|Mentioned|Fig.2,p163|Late Triassic|Middle Triassic|||||||01-MAR-10
3892|Challis Formation|60634|6|Mentioned|p1168 Fig.3. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Pollard Formation. Is overlain by Nome Formation.||
3892|Challis Formation|61548|6|Mentioned|p480 Fig.3|Carnian|Carnian|Northern Bonaparte Basin.||||||
3892|Challis Formation|61550|6|Mentioned|p495 Fig.2. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Pollard Formation. Is overlain by Nome Formation.||
3892|Challis Formation|62837|5|Briefly described|Stratigraphic columns|Late Triassic|Late Triassic|Of the Sahul Group.  Age: 225-~213Ma. Geological Province:  Vulcan Sub-basin (Western Bonaparte Basin).||||||01-MAR-10
3892|Challis Formation|63358|5|Briefly described|p4 Fig. 1.3|Norian|Carnian|||||||01-MAR-10
3892|Challis Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine sediments.||||Overlies Pollard Formation. Is overlain by Nome Formation.||
3892|Challis Formation|64689|5|Briefly described|p13 Fig.13|||||||Overlies Pollard Formation. Is overlain by Nome Formation.||
3892|Challis Formation|64693|6|Mentioned|p375|Triassic|Triassic|||||Is overlain unconformably by Nome Formation.||
3892|Challis Formation|64697|6|Mentioned|p87|Triassic|Triassic|Reservoir for Challis field.||||||
3892|Challis Formation|66124|5|Briefly described|p171 Fig.2|Carnian|Norian|Ashmore Platform (East). Marine, contains conodonts. Underlies Nome Formation and overlies Pollard Formation.||||||
3892|Challis Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Carnian||Sahul Group. Underlies the Nome Formation, overlies the Pollard Formation. Mount Ashmore Dome. Massive limestone. Mis-spelt as Chalis in Fig.2.||||||
3892|Challis Formation|68223|6|Mentioned|p178 Fig.3|Carnian|Carnian|||||||
3892|Challis Formation|69297|6|Mentioned|p305|Norian|Carnian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Sahul Group||Overlies the Pollard Formation. Overlain by the Nome Formation.|Sandstone and mudstone.|
3892|Challis Formation|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||||12-JUL-16
3892|Challis Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||||
3892|Challis Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p11|Norian|Norian|See also Vulcan: Fig.2, p2. Petroleum reservoir. Shallow marine, estuarine to intertidal. Potential oil reservoir in Vulcan Sub-basin.||Sahul Group.||Overlies Pollard Formation. Is overlain by Nome Formation.||12-JUL-16
3892|Challis Formation|70064|5|Briefly described|Regional Fig. 6. Central Fig.2|Norian|Carnian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Sahul Group.||Overlies Pollard Formation. Is overlain by Nome Formation.||12-JUL-16
3926|Charteris Basalt|22642|5|Briefly described|485|||Geol province Pilbara Craton||||||
3926|Charteris Basalt|24025|4|Described|p8 Tb. 1|Archean|Archean|Pillow basalt and minor high-Mg basalt.  Max. thickness: 1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
3926|Charteris Basalt|24184|5|Briefly described|p701|Archean|Archean|Of the Warrawoona Group. Underlain by Wyman Formation. Geological Province: Pilbara Craton. Reassigned from the Gorge Creek Group (Hickman 1983) to the Warrawoona Group||||||07-NOV-08
3926|Charteris Basalt|24531|5|Briefly described|p5 Tb. 1|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group).  Geological Province: Pilbara Craton.||||||07-NOV-08
3926|Charteris Basalt|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Kelly Subgroup (Warrawoona Group). Komatiite, basalt. Geological Province: Pilbara Craton.||||||07-FEB-11
3926|Charteris Basalt|31853|6|Mentioned|p60|||To be described by Hickman||||||
3926|Charteris Basalt|38498|5|Briefly described|Table 1|||||||||
3926|Charteris Basalt|38544|6|Mentioned|Fig.1|||||||||
3926|Charteris Basalt|39426|2|Defined|Table 1|Archean|Archean|||||||07-NOV-08
3926|Charteris Basalt|39697|4|Described|p99|||||||||
3926|Charteris Basalt|43595|6|Mentioned|p213|||||||||
3926|Charteris Basalt|43698|6|Mentioned|p3|||||||||
3926|Charteris Basalt|43779|5|Briefly described|p7|||||||||
3926|Charteris Basalt|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p134-135|||See also p139 Tb.2-18, p152 Tb.2-22. Recognised in only 2 areas. Original thickness < 1 km.||Soanesville Subgroup||Conformably overlies Corboy Formation.|Tholeiitic and high-Mg pillow lavas,  and dolerite sills; thin units of felsic lava and chert near the top.|
3926|Charteris Basalt|46922|6|Mentioned|p259|||Trace element analysis.||||||
3926|Charteris Basalt|61253|5|Briefly described|p51, p52 Fig. 2|Archean|Archean|Previously of the Kelly Subgroup (Warrawoona Group). Now of the Kelly Group (Pilbara Supergroup).  Geological Province: Pilbara Craton.||||||07-NOV-08
3926|Charteris Basalt|63245|5|Briefly described|p5|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Age: ca.3.43-3.32Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
3926|Charteris Basalt|63417|5|Briefly described|Map legend|Archean|Archean|Of the Kelly Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Basalt and basaltic komatiite; minor dolerite sills, chert and felsic volcanic rocks; metamorhposed.||||||07-NOV-08
3926|Charteris Basalt|63441|5|Briefly described|p4 Tb. 1|Archean|Archean|Of the Kelly Group (Pilbara Supergroup).||||||07-FEB-11
3926|Charteris Basalt|63538|4|Described|p5, p8 Tb. 1, p10, p6 Fig. 3|Archean|Archean|Of Kelly Group. Underlain by Wyman Formation. Geological Province: Pilbara Craton. Basaltic volcanism.||||||19-APR-13
3926|Charteris Basalt|64328|5|Briefly described|p54, p57|Archean|Archean|Of Kelly Subgroup (Warrawoona Gp) due to revised interpretation; previously part of Gorge Creek Gp. Conformable on Wyman Fm; unconformable below Gorge Creek Gp rocks. Age:c.3320 (nferred). Max. thickness: 2km. Mainly pillowed high Mg + tholeiitic basalt||||||07-FEB-11
3926|Charteris Basalt|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness: 1km.||||||07-FEB-11
3926|Charteris Basalt|64405|6|Mentioned|p4 Fig. 3, p21|||Komatiite basalt. See also p4 Fig. 3.||||||07-FEB-11
3926|Charteris Basalt|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Kelly Subgroup. Geological Province: Pilbara Craton. Basalt interlayered with dolerite and minor komatiitic basalt; metamorphosed.||||||07-FEB-11
3926|Charteris Basalt|65008|4|Described|p7, p8, p8 Fig.5, p10, p11, p14, p41|Paleoarchean|Paleoarchean|East Pilbara Granite-Greenstone Terrane. Includes 2 separately mapped facies. ~1km thick.|3325-3319 Ma|Of the Kelly Subgroup||Unconformably overlain by the Budjan Creek Formation?, Gorge Creek Group, Fortescue Group, and Corboy Formation. Conformably underlain by the Wyman Formation.|Basalt interlayered with dolerite and minor komatiitic basalt; komatiitic basalt and minor basalt, numerous pillows. Both metamorphosed.|14-MAY-14
3926|Charteris Basalt|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton. Mapped as five sub-units.||Of Kelly Subgroup.|||Tholeiitic basalt interlayered with dolerite and komatiitic basalt; komatiitic basalt with numerous pillows; dolerite; fine-grained, silicified, felsic tuff and tuffaceous sandstone; chert; all metamorphosed.|
3926|Charteris Basalt|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as five sub-units.||Of Kelly Group.|||Tholeiitic basalt interlayered with dolerite and komatiitic basalt; komatiitic basalt with numerous pillows; dolerite; fine-grained, silicified, felsic tuff and tuffaceous sandstone; chert; all metamorphosed.|
3926|Charteris Basalt|65827|3|Fully described|p6 Tb.1, p21, p22, p29, p31,|Paleoarchean|Paleoarchean|Of Kelly Group. Unconformably underlies/faulted against Budjan Creek Formation, Gorge Creek Group, Fortescue Group; conformably overlies Wyman Formation; faulted against by Euro Basalt; unconformably underlies Farrel Quartzite. Age not yet determined.||||||
3926|Charteris Basalt|65829|6|Mentioned|p9. |||||Unit in Kelly Group.||||
3926|Charteris Basalt|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Kelly Group. Basalt and basaltic komatiite; minor dolerite sills, chert, and felsic volcanic rocks; metamorphosed.||||||
3926|Charteris Basalt|66217|5|Briefly described|p8, p29.|||Van Kranendonk et al. (2002) included this unit in the Kelly Subgroup in their redefinition of the Warrawoona Group. Locally 1000 m thick.||||Conformably overlies Wyman Formation.||
3926|Charteris Basalt|66745|4|Described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Hydrothermal gold mineralization. Its formation was followed by a major event of vertical deformation (doming) and regional metamorphism (c.3290-3270 Ma).||Unit in Kelly Group.||Overlies Wyman Formation. Is unconformably overlain by Leilira Formation.|Basalt, komatiitic basalt; minor felsic volcanic rocks.|
3926|Charteris Basalt|67130|5|Briefly described|p16|||Up to 1000m thick.||||Conformably overlies Wyman Formation|Basalt.|
3926|Charteris Basalt|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Kelly Group.||||
3926|Charteris Basalt|67201|5|Briefly described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.||Kelly Group||||
3926|Charteris Basalt|67269|5|Briefly described|p6 Fig.3|Paleoarchean|Paleoarchean|||Kelly Group.||Overlies Wyman Formation. Is overlain unconformably by Leilira Formation.|Basalt; minor felsic volcanic rocks.|
3926|Charteris Basalt|67270|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Kelly Group.||||
3926|Charteris Basalt|67668|6|Mentioned|Fig. 2;||Paleoarchean|East Pilbara Terrane, Pilbara Craton.||Kelly Group||Overlies the Wyman Formation, unconformably underlies the Leilira Formation (Sulphur Springs Group).||
3926|Charteris Basalt|68035|4|Described|p288 Fig 4|Paleoarchean|Paleoarchean|Pilbara Supergroup, East Pilbara Terrane.||Of Kelly Group.||Overlies Wyman Formation. Unconformably overlain by Leilira Formation, Sulphur Springs Group.|Komatiitic basalt, basalt, minor felsic volcanics|
3926|Charteris Basalt|68280|5|Briefly described|p4|||||Kelly Group||Unconformably overlain by Leilira Formation, overlies Wyman Formation|Basalt, komatiitic basalt and felsic volcanic rocks.|
3926|Charteris Basalt|68284|5|Briefly described|p4, 7|Paleoarchean|Paleoarchean|Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|c.3300 Ma.|Kelly Group.||Overlies Wyman Formation. Is overlain by Leilira or Budjan Creek Formations.|Similar composition to Euro Basalt: komatiite, komatiitic basalt, numerous thin chert units, and local clastic and volcaniclastic sedimentary rocks.|
3926|Charteris Basalt|69012|6|Mentioned|Map Legend|Archean|Archean|East Pilbara Terrane.||Unit in Kelly Group.||||29-APR-14
3926|Charteris Basalt|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|||Kelly Group|||Felsic volcanic sandstone, tuffaceous; metamorphosed. Dolerite, tholeiitic basalt,pillowed and massive komatiitic basalt and komatiite with pyroxene and olivine spinifex textures.|
3926|Charteris Basalt|69301|4|Described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. East Pilbara Terrane.||Kelly Group|||Basalt, komatiite; with felsic volcanic rocks.|
3926|Charteris Basalt|69566|5|Briefly described|p236-237, 246|||Hickman (1984). East Pilbara Granite-Greenstone Terrane. Presented as Charteris Formation in places in the text.|3315-3312 Ma (Hickman, 1984).|Kelly Group.||Conformably overlies Wyman Formation. Is overlain by Budjan Creek Formation (George Creek Group).||
3926|Charteris Basalt|69590|4|Described|GEOL_LUT_CSV files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv.|3325-3315 Ma (inferred)|Unit of Kelly Group.|||Tholeiitic basalt, interlayered dolerite and komatiitic basalt; metamorphosed; komatiite with pyroxene and olivine-spinifex textures; metamorphosed; felsic volcanic sandstone, tuffaceous; metamorphosed.|
3926|Charteris Basalt|70022|6|Mentioned|p115|||East Pilbara Terrane.||Kelly Group.||||
3926|Charteris Basalt|70775|5|Briefly described|p12|||East Pilbara.||Kelly Group||Overlies the Wyman Formation. Unconformably overlain by the Leilira Formation.||
3926|Charteris Basalt|70884|5|Briefly described|p123|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Overlain unconformably by Leilira Formation/Sulphur Springs Group. Underlain by Wyman Formation.||
3926|Charteris Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Kelly Large Igneous Province, East Pilbara Terrane.||Kelly Group|||Basalt and basaltic komatiite; minor dolerite sills, chert and felsic volcanic rocks; metamorphosed.|
3926|Charteris Basalt|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Uppermost unit of Kelly Group. Overlain by Leilira Formation/Kelly Group. Underlain by Wyman Formation.||
3926|Charteris Basalt|72251|5|Briefly described|p54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Kelly Group.||Uppermost unit of Kelly Group. Overlain unconformably by Leilira Formation. Underlain by Wyman Formation.||
3926|Charteris Basalt|72668|5|Briefly described|p4-6, p26|||East Pilbara Terrane. Locally 1000m thick.|c. 3350-3310 Ma|Kelly Group||Conformably overlies the Wyman Formation.||12-JAN-22
3926|Charteris Basalt|73598|5|Briefly described|p1208, 1211-1212|Paleoarchean|Paleoarchean|East Pilbara Terrane. REE diagrams. Fed by Kelly Dyke swarm dykes.||Kelly Group.||Overlies Wyman Formation. Is overlain by Leilira Formation.|Dolerites, with overall primitive geochemical signatures.|
3941|Cheela Springs Basalt|22484|5|Briefly described|p77 Fig.6|||||||||
3941|Cheela Springs Basalt|23046|6|Mentioned|178|||Parent Wyloo Group||||||
3941|Cheela Springs Basalt|23047|5|Briefly described|35|||Hamersley Province. Age 2209 +/-15 Ma. Overlain by Wooly Dolomite, underlain by Beasley River Quartzite.||||||10-FEB-09
3941|Cheela Springs Basalt|23280|5|Briefly described|p1085,1087,Fig2p1086||Rhyacian|Max Age: SHRIMP U-Pb 2209 (+/-) 15 Ma.||||||
3941|Cheela Springs Basalt|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
3941|Cheela Springs Basalt|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit Mount McGrath Formation. Underlying unit Beasley River Quartzite.||||||
3941|Cheela Springs Basalt|23612|5|Briefly described|p841|||||||||
3941|Cheela Springs Basalt|23774|5|Briefly described|p733 table 1||Paleoproterozoic|Age: 2209+/-5 Ma. Of Wyloo Group.||||||07-NOV-08
3941|Cheela Springs Basalt|23890|5|Briefly described|p5 Fig.2|||Age: 2209+/-15Ma (U-Pb SHRIMP).  Geological Province: Ashburton Basin.||||||
3941|Cheela Springs Basalt|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of Lower Wyloo Group. Conformably overlies Beasley River Quartzite. Conformably overlain by Wooly Dolomite. Age: 2209+/-15 Ma. Tholeiitic. Max. thickness: 2000 m. Geological Province: Ashburton Province.||||||07-NOV-08
3941|Cheela Springs Basalt|24602|5|Briefly described|p855 Fig. 2|||Of the Wyloo Group.||||||
3941|Cheela Springs Basalt|24607|4|Described|p967|Paleoproterozoic|Paleoproterozoic|The youngest components of zircons from volcaniclastic breccia in this unit  give an age of  2209 +/- 15 Ma, which is interpreted as close to the eruptive age of the continental tholeiitic basalt. Geological Province: Ashburton Basin.||Of the Wyloo Group||Overlies the Beasley River Quartzite. Unconformably overlain by the Mount McGrath Formation||30-NOV-10
3941|Cheela Springs Basalt|35218|6|Mentioned|p6|||||||||
3941|Cheela Springs Basalt|37327|6|Mentioned|p396|||||||||
3941|Cheela Springs Basalt|38321|6|Mentioned|Table 1|||||||||
3941|Cheela Springs Basalt|40103|6|Mentioned|Fig.1|||||||||
3941|Cheela Springs Basalt|40369|6|Mentioned|Plate 1|||||||||
3941|Cheela Springs Basalt|40905|6|Mentioned|Fig.1|||||||||
3941|Cheela Springs Basalt|40937|6|Mentioned|p28|||||||||
3941|Cheela Springs Basalt|41845|6|Mentioned|Fig. 1|||||||||
3941|Cheela Springs Basalt|41846|6|Mentioned|Fig.1|||||||||
3941|Cheela Springs Basalt|41955|6|Mentioned|Fig.1 P4|||||||||
3941|Cheela Springs Basalt|42148|6|Mentioned|p690|||||||||
3941|Cheela Springs Basalt|42260|3|Fully described|p27|||||||||
3941|Cheela Springs Basalt|42277|6|Mentioned|p55|||||||||
3941|Cheela Springs Basalt|42435|6|Mentioned|Fig.1 P43|||||||||
3941|Cheela Springs Basalt|42471|4|Described|p10|||||||||
3941|Cheela Springs Basalt|42472|5|Briefly described|Map legend|||||||||
3941|Cheela Springs Basalt|42686|5|Briefly described|map legend|Proterozoic||||||||
3941|Cheela Springs Basalt|42704|5|Briefly described|Plate 2E|Proterozoic||Of the Wyloo Group. Vesicular and amygdaloidal basalt.||||||07-AUG-08
3941|Cheela Springs Basalt|42744|4|Described|p6|||||||||
3941|Cheela Springs Basalt|43037|6|Mentioned|Table 1,p24|||of Wyloo Group||||||
3941|Cheela Springs Basalt|43119|5|Briefly described|p13|||of Wyloo Group||||||
3941|Cheela Springs Basalt|43262|5|Briefly described|Map Legend||Proterozoic|of Wyloo Group||||||
3941|Cheela Springs Basalt|43290|4|Described|p9||Proterozoic|of Wyloo Group. Formerly of Mount McGrath Formation.||||||
3941|Cheela Springs Basalt|44152|6|Mentioned|p188 Fig.2-161|||||Wyloo Group.||Overlies Beasley River Quartzite.||
3941|Cheela Springs Basalt|50216|5|Briefly described|p208|Paleoproterozoic|Paleoproterozoic|Of the lower part of Wyloo Group. Age: ca. 2200 Ma (Martin et al., 1988). Geological Province: Ashburton Basin.||||||07-NOV-08
3941|Cheela Springs Basalt|50223|5|Briefly described|p356|Paleoproterozoic|Paleoproterozoic|Age: 2.2Ga (Martin, 1998).  Geological Province: McGrath Trough, Hamersley Province.||||||01-MAR-10
3941|Cheela Springs Basalt|50226|5|Briefly described|p415|Paleoproterozoic|Paleoproterozoic|Of the Wyloo Group.  Age: 2.2Ga (Martin et al, 2000).  Geological Province: Ashburton Basin.||||||07-NOV-08
3941|Cheela Springs Basalt|50227|5|Briefly described|p445|Mesoproterozoic|Mesoproterozoic|Age: 2209Ma.||||||07-FEB-11
3941|Cheela Springs Basalt|61276|4|Described|p577-580|Orosirian|Orosirian|Max Thickness: 2700m. Flood Basalt. Cut by a NW trending dyke in Hardy syncline with SHRIMP Pb/Pb baddelyite age of 2007 +/-16 Ma. Zircon age of sedimentary breccia in this unit (2209 +/-15 Ma) is here reinterpreted to be a provenance age. Conformably overlain by tuffaceous siltstone of the Wooly Dolomite dated at 2031+/-6 Ma as volcaniclastic sedimentation.||Of the Wyloo Group.||Overlies Beasley River Quartzite. Underlies the Wooly Dolomite conformably, so can't be much older.||17-OCT-16
3941|Cheela Springs Basalt|61526|5|Briefly described|p879, p882|Paleoproterozoic|Paleoproterozoic|Of the Lower Wyloo Group. Overlies Beasley River Quartzite. Age: <2.2Ga. See also p883.||||||07-NOV-08
3941|Cheela Springs Basalt|62129|3|Fully described|p14, p20|Proterozoic|Proterozoic|Of Wyloo Group. Comformably underlain by Beasley River Quartzite. Thickness: 1700m. Geological Province: Ashburton Basin. Basalt flows interbedded with minor amounts of flow top breccia and parallel-laminated dolomite. See p 14-15 for more detailed info.||||||07-FEB-11
3941|Cheela Springs Basalt|62130|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Geological Province: Ashburton Basin. Metamorphosed amygdaloidal basalt flows and metabasaltic breccia, pelite, metasandstone and metadolomite.||||||23-DEC-09
3941|Cheela Springs Basalt|63866|5|Briefly described|p154|||||||Overlies the Beasley River Quartzite. (Partially) overlain by the Wooly Dolomite.||
3941|Cheela Springs Basalt|63869|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|SHRIMP U-Pb maximum age from detrital zircons from a volcaniclastic breccia.|<2209 +/- 15 Ma (Martin et al., 1998).|Unit in Wyloo Group.||||
3941|Cheela Springs Basalt|64384|5|Briefly described|p46, p47 Tb. 7|||Of Wyloo Group. Overlies Beasley River Quartzite; disconformably overlain by Mount McGrath Fm. Mainly vesicular basalt but includes subordinate fine- to coarse-grained tuff, immature sandstone, and mudstone. See also p63-4, p83.||||||07-FEB-11
3941|Cheela Springs Basalt|64580|6|Mentioned|map legend|||Of Wyloo Group, Lower.||||||15-DEC-08
3941|Cheela Springs Basalt|64724|5|Briefly described|p43|Orosirian|Orosirian|Cross-cut by 2008 +/- 16 Ma dykes.||Of Wyloo Group.||||02-APR-12
3941|Cheela Springs Basalt|64728|6|Mentioned|p97.|||||||||
3941|Cheela Springs Basalt|65692|5|Briefly described|p2, p31|||Northern Hamersley Province, Pilbara Craton. Suggested as a possible source for some Earaheedy Basin sediments.|c.2.2 Ga (zircons; Martin et al., 1998).|||||
3941|Cheela Springs Basalt|65830|6|Mentioned|p3|||||Of the Wyloo Group||Underlain by the Beasley River Quartzite.||
3941|Cheela Springs Basalt|66115|5|Briefly described|p136, p137 Fig.1|Paleoproterozoic|Paleoproterozoic||2209+/-15 Ma SHRIMP U-Pb, Martin et al. 1998|Wyloo Group||||
3941|Cheela Springs Basalt|66359|5|Briefly described|e96|||Said by Martin to overlie dolerite-hosting quartzites in Turee Creek syncline. Intruded by undated dolerite sills. Dated at 2209 +/-15 Ma (Martin, 1998). Muller et al say this unit is not present in Turee Creek syncline, only dolerite float.||Near base of Wyloo Group.||Overlies Beasley River Quartzite.||19-SEP-13
3941|Cheela Springs Basalt|66574|5|Briefly described|p911, p914 Fig.3, p916 Fig.4||Rhyacian|Part of lower Wyloo Group. Thick succession of continental-arc tholeiitic amygdaloidal basalts: 75 flows, average  thickness of 30m. McGrath Trough. Underlies Wooly Dolomite, overlies Beasley River Quartzite and Nummana Member. 2209 +/- 15 Ma.||||||
3941|Cheela Springs Basalt|66887|5|Briefly described|p21 Fig.11|||Ashburton Basin. Pilbara Craton.|~2200 Ma estimated from Fig.11.|Wyloo Group, lower||||
3941|Cheela Springs Basalt|66950|5|Briefly described|p4|Rhyacian|Rhyacian||c. 2210 Ma (Martin et al. 1998)|||Underlain by the Beasley River Quartzite.||
3941|Cheela Springs Basalt|67025|5|Briefly described|pp319-320, pp322-324.|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.||||
3941|Cheela Springs Basalt|67056|5|Briefly described|p419 Fig.2. |Paleoproterozoic|Paleoproterozoic||2209 Ma.|Unit in Lower Wyloo Group.||Overlies Beasley River Quartzite. Is overlain by Wooly Dolomite.||
3941|Cheela Springs Basalt|67130|5|Briefly described|p3 fig 2, p4-6, p24-25|Rhyacian|Rhyacian|Maximum of 2km  thick. Plagioclase phyric basalt up to 35m thick. Can be geochemically divided into two parts with distinct compositions. See also p24 fig 17, p25, p39 fig 36.|2208 +/- 16 Ma|Wyloo Group, Lower||Conformably overlies Beasley River Quartzite, Nummana Member, conformably overlain by Wooly Dolomite|Vesicular basalt, doleritic basalt and rare plagioclase-phyric basalt.|
3941|Cheela Springs Basalt|67201|5|Briefly described|p35||||~ 2210 Ma|In lower Wyloo Group||||
3941|Cheela Springs Basalt|67843|6|Mentioned|p33.|||Ashburton Basin.||Unit in Wyloo Group.||||
3941|Cheela Springs Basalt|67855|4|Described| p213-214, p212 fig 3-10, p228, p231|Paleoproterozoic|Paleoproterozoic|Of Horwitz (1980). Up to 2km thick. Previously a member within the Mount McGrath Formation. Coastal to shallow marine environment.||Wyloo Group. Previously part of Mount McGrath Formation.||Conformably overlies Beasley River Quartzite, disconformably overlies Mount Bruce Supergroup.|Basalt flows (0.5 to 35m thick) with subordinate tuff, immature sandstone, siltstone, and mudstone. Many dolerite sills (to 50m thick).|
3941|Cheela Springs Basalt|68035|4|Described|p293, p292 fig 6|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.  Up to 2 km thick. Cut by dolerite dykes emplaced at 2.01 Ga.|2208 +/- 16 Ma|Of lower Wyloo Group.||Conformably overlies Beasley River Quartzite. Overlain by Wooly Dolomite?|Basalt derived from a subduction-modified source.|
3941|Cheela Springs Basalt|68280|5|Briefly described|p5, p51, p54, p62|Paleoproterozoic|Paleoproterozoic||2208+/- 16 Ma||Includes Nummana Member, Beasley River Quartzite, Three Corners Conglomerate Member|Overlain by Wooly Dolomite, Unconformably overlies Kazput Formation|Vesicular basalt.|13-JAN-23
3941|Cheela Springs Basalt|69003|5|Briefly described|p4, p7-8|||Capricorn Orogen. Foredeep mafic volcanism. c.2.5 km thick. Coeval with dolerite sills that intrude the Turee Creek Group.||||Conformably overlies Beasley River Quartzite. Is overlain conformably by Wooly Dolomite or unconformably by upper Wyloo Group.|Continental tholeiite lavas.|
3941|Cheela Springs Basalt|69028|5|Briefly described|Map Legend|Orosirian|Rhyacian|Ashburton and Blair Basins. Mapped with Beasley River Quartzite and Wooly Dolomite as a single unit.||Of the Wyloo Group, lower.|||Conglomerate, sandstone, mudstone, basalt, chert and locally stromatolitic dolomite.|07-MAY-14
3941|Cheela Springs Basalt|69080|5|Briefly described|p686 Fig.4, p687|Rhyacian|Rhyacian|Southern Pilbara. c.2 km thick. Age inferred from Fig.4, but text states c. 2210 Ma.|c.2140 Ma.|Unit in Wyloo Group.||||
3941|Cheela Springs Basalt|69166|6|Mentioned|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Wyloo Group||||
3941|Cheela Springs Basalt|69185|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic|Of Ashburton Basin.||Unit of Wyloo Group.||||
3941|Cheela Springs Basalt|69538|6|Mentioned|p517 Fig.3|Paleoproterozoic|Paleoproterozoic|||Unit in Wyloo Group.||||
3941|Cheela Springs Basalt|69565|6|Mentioned|p133 Fig.1|||Hamersley Province.|2209 +/- 15 Ma.|Wyloo Group.||Overlies Beasley River Quartzite. Is overlain by Mount McGrath Formation.||
3941|Cheela Springs Basalt|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Wyloo Group, Lower.||||
3941|Cheela Springs Basalt|69596|5|Briefly described|p5, p7|Rhyacian|Rhyacian|Southern Pilbara.|c.2210 Ma.|Lower Wyloo Group.||||
3941|Cheela Springs Basalt|69745|6|Mentioned|p273, 275, 281, 283, 286-287|||Hamersley Province. Is presented as Cheela Springs Formation on pp273, 275, 286, 287.||Lower Wyloo Group.|||Volcanic rocks.|
3941|Cheela Springs Basalt|69754|6|Mentioned|p316-p317, p340|Rhyacian|Rhyacian|Pilbara Craton.|2209 +/- 15 Ma|Wyloo Group||Unconformably overlies the Kungarra Formation.||
3941|Cheela Springs Basalt|70086|5|Briefly described|p195-196,209|Rhyacian|Rhyacian|Geological province: Pilbara Craton. Of the Hamersley Basin. Muller et al., 2005 interpreted 2209+\-15 Ma to reflect provenance, however also provided U-Pb baddeleyite of 2208+\-15 Ma for diorite sills that cut the Turee Creek Group, an essentially indistinguishable minimum age constraint.|2209+\-15 Ma|Unit of Wyloo Group.||Overlain by Mount McGrath Formation. Underlain by Nummana Member/Beasley River Quartzite.||
3941|Cheela Springs Basalt|70327|4|Described|p1-4, p6, p8-16, p18-19|||Horseshoe Basin, Ashburton Province. Flood basalts, ~2.7 km thick. Locally tightly folded. The age determination of 2209 +/- 15 Ma (Martin et al., 1998), from detrital zircons in a conglomerate near the top of this unit, is c.170 m.y. older than the syneruptive c.2031 Ma age determined by Muller et al. (2005). The Cheela Springs Basalt is also younger than the 2195-2145 Ma Ophthalmia Orogeny. It is cut by a ~2008 Ma dyke swarm.|~2145 - ~2008 Ma.|||Conformably overlies Beasley River Quartzite. Is overlain conformably by Wooly Dolomite and unconformably by Mount McGrath Formation.|Flood basalt, amygdaloidal basalt interlayered with conglomerate.|
3941|Cheela Springs Basalt|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Turee Creek Basin|2208 Ma||||Amygdaloidal metabasalt; minor interbedded tuff, immature sandstone, siltstone and mudstone; dolerite sills.|
3941|Cheela Springs Basalt|70949|5|Briefly described|p988-989|Paleoproterozoic|Paleoproterozoic|||Shingle Creek Group.|||Basalt, subordinate tuff and sandstone.|
3941|Cheela Springs Basalt|70958|4|Described|p4, p15 App. 1, p16, Fig. 1|Paleoproterozoic|Paleoproterozoic|Previously considered a basal member of the Mount McGrath Formation, but here excluded and raised to Formation status because top contact is disconformable. Said to be redefined, but no type section given. 900 m thick around Cheela Springs. Thicker at Mount Maguire.||Of Wyloo Group||Overlies Beasley River Quartzite. Disconformably overlain by Mount McGrath Formation.|Basal tuffaceous-looking shales; several flows of vesicular basalt. Some shales bands and chert nodules.|
3941|Cheela Springs Basalt|71112|4|Described|p69-70,74-77,79-80,82-83,87|Rhyacian|Rhyacian|Geological province: Ashburton Province, Pilbara Craton. Of the Horseshoe Basin (intracontinental rift basin). Flood basalt province.  Contains 2215 Ma zircon ages, indicating possible input from a bimodal igneous province.|<2209+\-15 Ma|||Ovelain by Wooly Dolomite. Underlain by Beasley River Quartzite.|Interlayering of basalt, basaltic hyaloclastite, volcaniclastic mudstone and clastic dolostone.|
3941|Cheela Springs Basalt|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||ash tuff, sandstone, basalt|
3941|Cheela Springs Basalt|71550|5|Briefly described|p35-37,45|Rhyacian|Rhyacian|Geological province: Of Hamersley Basin. Contains U-Pb zircon dates at 2209+\-15 Ma (Martin et al., 1998), interpreted to be a maximum depositional age as the age was based on potentially detrital zircons from volcanic breccia (Muller et al., 2005).||Unit of lower Wyloo Group.||Underlain by Beasley River Quartzite.||03-SEP-19
3941|Cheela Springs Basalt|71808|6|Mentioned|p48, p74, p149, p156|||Date derived from a volcanogenic breccia however the relevance of this date is open to interpretation.|2209 +/- 15 Ma (Martin et al, 1998b)|||Overlies the Beasley River Quartzite.||
3941|Cheela Springs Basalt|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Turee Creek Basin.||Shingle Creek Group||Intruded by Balgara Dolerite sills.|Amygdaloidal basalt and minor volcaniclastic rock; immature sandstone, siltstone, and mudstone; intruded by Balgara Dolerite sills.|
3941|Cheela Springs Basalt|72570|6|Mentioned|p2|Rhyacian|Rhyacian||2209 +/- 15 Ma|Shingle Creek Group||Overlies the Beasley River Quartzite.||
3941|Cheela Springs Basalt|72712|5|Briefly described|p5, p9, p31, p33, p36 Fig.25, p41|Rhyacian|Rhyacian|Previously called Cheela Springs Basalt Member. Type section near Shingle Creek (Dow, 1996) where it is 2890m thick and consists of 75 tholeiitic basalt flows averaging 30m thickness. locally interbedded fine-grained turbidites, hyaloclastite breccia, and peperite support interpretation of subaqueous emplacement. SHRIMP dating was on volcaniclastic breccia horizon. Age interpreted to be close to depositional age. Petrogenetically related to Balgara Dolerite. See also p30, p42-p43, p45, p53, p54, p55.|MDA 2203 +/-4 Ma SHRIMP U-Pb zircon.|Shingle Creek Group|Nummana Member|Unconformably overlain by Mount McGrath Formation. Intruded by dolerite sills.|Contains basalt flows and thick dolerite sills with locally vesicular tops. Late deposits of ferruginous argillite with minor sandstone, conglomerate and chert, locally with cobble to boulder-sized clasts of dolomite form the upper unconformity.|14-JAN-21
3941|Cheela Springs Basalt|72758|5|Briefly described|p13 Tb.1, p31-34, p38, p40.|Paleoproterozoic|Paleoproterozoic|Up to 2000m thick. Basalt flows from 0.5 to 35m thick. Possible feeder conduit, separated from main outcrop, at 22deg 23' 40"" S, 116deg30' E. Thins to nothing way from type locality. Previously regarded as a member of the Mount McGrath Formation. Coastal to shallow marine environment interpreted from setting.||Wyloo Group||Conformably overlies Beasley River Quartzite. Disconformably overlies Mount Bruce Supergroup. Conformably overlain by Wooly Dolomite, disconformably overlain by Mount McGrath Formation.|Vesicular and amygdaloidal basalt (mostly metamorphosed) with minor tuff and chert, immature sandstone, siltstone and mudstone; some dolerite sills.|
3950|Cherrabun Member|22741|5|Briefly described|P29, Table3 p12||Permian|||||||04-NOV-15
3950|Cherrabun Member|22767|5|Briefly described|Table3 P14, P22||Late Permian|||||||
3950|Cherrabun Member|22776|4|Described|Table.3|Late Permian|Late Permian|Hardman Formation, Liveringa Group||||||
3950|Cherrabun Member|30342|6|Mentioned|Table 20|||||||||
3950|Cherrabun Member|33518|4|Described|Table 1|||||||||
3950|Cherrabun Member|33519|6|Mentioned|Map legend|Permian|Permian|||||||
3950|Cherrabun Member|33962|2|Defined|p51|Permian|Permian|||||||
3950|Cherrabun Member|36224|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Hardman Formation (Liveringa Group).  Mudstone, calcareous, fossiliferous; sandstone, cross-bedded; minor limestone.||||||01-FEB-05
3950|Cherrabun Member|36225|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
3950|Cherrabun Member|36634|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
3950|Cherrabun Member|41158|6|Mentioned|p162|||||||||
3950|Cherrabun Member|41540|5|Briefly described|p21|||||||||
3950|Cherrabun Member|41688|6|Mentioned|p10|||||||||
3950|Cherrabun Member|42540|5|Briefly described|p314|||of Hardman Formation.||||||
3950|Cherrabun Member|42654|6|Mentioned|p20|||of Hardman Formation||||||
3950|Cherrabun Member|43015|5|Briefly described|Table 1,p319|||of Hardman Formation||||||
3950|Cherrabun Member|45153|4|Described|App.4-78|||See also App.4-73.||||||
3950|Cherrabun Member|45158|4|Described|p18|||||||||
3950|Cherrabun Member|49644|5|Briefly described|Table|||||||||
3950|Cherrabun Member|64974|6|Mentioned|p148 Fig. 6|Tatarian|Tatarian|Of Hardman Formation. Geological Province: Canning Basin.||||||24-JUN-09
3950|Cherrabun Member|66949|4|Described|p4 Fig.2, p25-26, p55 Appx.3|Wuchiapingian|Wuchiapingian|Type section detailed. Up to 100m thick; regressive marine deposits. Age from macrofauna. Biostratigraphic zonation.||Uppermost unit in Hardman Formation.||Overlies Hicks Range Sandstone Member.|Sandstone (locally richly fossiliferous), laminated siltstone and rare limestone.|04-NOV-15
3950|Cherrabun Member|70774|5|Briefly described|p9|Wuchiapingian|Wuchiapingian|||Hardman Formation.||Overlies the Hicks Range Member.||10-FEB-20
3950|Cherrabun Member|71623|5|Briefly described|p343, 349, p345 fig 5||Wuchiapingian|Canning Basin. Marine. Contains ammonite Cyclolobus persulcatus which establishes a correlation with the Salt Range area.||Of Hardman Formation.||Overlies the Hicks Range Member.|Limestone|08-MAY-19
3951|Cherrybooka Conglomerate|36883|3|Fully described|p144|||||||||
3951|Cherrybooka Conglomerate|36902|6|Mentioned|p15|||||||||
3951|Cherrybooka Conglomerate|37460|5|Briefly described|p156|||||||||
3951|Cherrybooka Conglomerate|38482|6|Mentioned|p15|||||||||
3951|Cherrybooka Conglomerate|40554|5|Briefly described|p30|||||||||
3951|Cherrybooka Conglomerate|41125|6|Mentioned|p28|||||||||
3951|Cherrybooka Conglomerate|42260|6|Mentioned|p100|||||||||
3951|Cherrybooka Conglomerate|42471|6|Mentioned|p18|||Used 1965||||||
3951|Cherrybooka Conglomerate|44141|6|Mentioned|p304-308|||The Cherrybooka Conglomerate and Kunderong Sandstone intergrade laterally and vertically; therefore they are not clearly mappable.||Bresnahan Group||Is overlain gradationally by Kunderong Sandstone.||
3951|Cherrybooka Conglomerate|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Bresnahan Basin. Mapped with Kunderong Sandstone as a single unit, so lith. description applies to both.||Of the Bresnahan Group.|||Pebble- to boulder-conglomerate, pebbly sandstone, sandstone, siltstone and mudstone.|18-SEP-15
4002|Chimney Rock Oolite|36890|4|Described|p356|||||||||
4002|Chimney Rock Oolite|44998|2|Defined|p.197||Cenozoic|Overlies Emeriau Sandstone.||||||19-NOV-08
4002|Chimney Rock Oolite|45153|2|Defined|App.11-164|Pleistocene|late Tertiary|Possibly Late Tertiary to Pleistocene||||||
4002|Chimney Rock Oolite|64449|5|Briefly described|p62 Tb. 2, p63|Quaternary|Quaternary|Consists of clacerted, well cemented oolitic limestone.||||||07-FEB-11
4033|Chocolate Hill Formation|30766|6|Mentioned|p7|||Refers Ingram (1972). Subdivision of Warrawoona Succession||||||
4033|Chocolate Hill Formation|37373|4|Described|p75|||||||||
4033|Chocolate Hill Formation|39697|6|Mentioned|Table 3|||||||||
4033|Chocolate Hill Formation|44150|6|Mentioned|p133 Tb.2-16|||East Pilbara. Of Ingram (1977). Probably obsolete; currently appears to be divided into North Star Basalt and McPhee Formation. ||||||
4046|Christmas Creek Member|7433|5|Briefly described|p34, p36. |||Restricted to Fitzroy Sub-basin in Canning Basin. Fluvial coarse-clastic facies.||Uppermost unit in Poole Sandstone.||Overlies Tuckfield Member.||
4046|Christmas Creek Member|22741|5|Briefly described|p27, Table3pP13||Permian|||||||10-FEB-20
4046|Christmas Creek Member|24466|5|Briefly described|p365|Early Permian|Early Permian|Of the Poole Sandstone.  Conformably overlies Tuckfield Member.||||||
4046|Christmas Creek Member|30338|2|Defined|p102|Artinskian|Artinskian|||||||
4046|Christmas Creek Member|30342|6|Mentioned|Table 20|||||||||
4046|Christmas Creek Member|36225|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
4046|Christmas Creek Member|42613|5|Briefly described|p14|||||||||10-FEB-20
4046|Christmas Creek Member|45158|4|Described|p20|||||||||
4046|Christmas Creek Member|64643|4|Described|p21, fig.18 p23|||Of Poole Sandstone. Type section at Mount Piper, Poole Range. Medium to coarse-grained cross-bedded sandstone.||||||
4046|Christmas Creek Member|66949|4|Described|p20, p23, p56 Appx.3|Artinskian|Artinskian|Type section detailed. Up to 25m thick; fluvial deposits. Continuity in question as unit is cut out by channel within 500 m of type section. Validity as mappable unit questioned. Unlikely to be identifiable in subsurface.||Upper Member of Poole Sandstone.||Similar to Tuckfield Member.|Sandstone and pebbly sandstone.|02-NOV-15
4046|Christmas Creek Member|70774|5|Briefly described|p7|||Previously the upper sub-division of the Poole Sandstone before being suggested to be    unecessary by Mory (2010).||||||10-FEB-20
4067|Cistern Formation|22499|6|Mentioned|p10-13|||||||||
4067|Cistern Formation|23244|5|Briefly described|Fig.2,5 p19|||of Whim Creek Group, Whim Creek Belt.||||||
4067|Cistern Formation|23348|5|Briefly described|220|||||||||
4067|Cistern Formation|23484|4|Described|p10 table 3|Archean|Archean|Of Whim Creek Group.  Maximum thickness:  ~100m.  Geological Province: Mallina Basin.||||||07-NOV-08
4067|Cistern Formation|23598|5|Briefly described|p3|||Of Whim Creek Group. Geological Province: Pilbara Craton.||||||
4067|Cistern Formation|23743|5|Briefly described|p4|Archean|Archean|Underlying unit Mons Cupri Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|23784|4|Described|p22|Archean|Archean|Of Bookingarra Group.  See also p28.||||||07-NOV-08
4067|Cistern Formation|23789|5|Briefly described|p18 Tb. 4|Archean|Archean|Of Bookingarra Group.  Max. thickness: 800m.  Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|23793|4|Described|p22|Archean|Archean|Of Whim Creek Group. Age: c. 2975Ma||||||07-NOV-08
4067|Cistern Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Whim Creek Group. Overlying unit Rushall Slate. Underlying unit Mons Cupri Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Of the Bookingarra Group.  Age: 2.965-2.95Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.3.01-2.99 Ga. Geological Province: Pilbara Craton. Overlain by Rushall Slate. Underlain by Mons Cupri Volcanics.||||||01-MAR-10
4067|Cistern Formation|24023|5|Briefly described|p18|||||||||
4067|Cistern Formation|24140|4|Described|p216, p214 Fig. 1|Archean|Archean|Of the Bookingarra Group (reclassified from Whim Creek Group). Volcaniclastic conglomerate, breccia and sandstone. Overlain by Rushall Slate; overlies Whim Creek Group. Intruded by Negri Volcanics. Max. thickness: 330m. Geological Province: Mallina Basin||||||07-NOV-08
4067|Cistern Formation|24184|4|Described|p715|Archean|Archean|Of the Bookingarra Group. Overlain by Rushall Shale. Geological Province: Mallina Basin. Age: >2970Ma. Formerly included in Whim Creek Group (Hickman 1983), now assigned to the Bookingarra Group||||||07-NOV-08
4067|Cistern Formation|24185|5|Briefly described|p739 Tb.3, p744 Tb.4|Archean|Archean|Minimum Age: 2964 +/- 6 Ma (SHRIMP zircon U-PB). Overlying Unit: Rushall Slate. Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|24191|4|Described|p828 Fig. 1|Archean|Archean|Of Bookingarra Group.  Overlain by Rushall Slate.  Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|24192|5|Briefly described|p860|Archean|Archean|Parent: Bookingarra Group. Geological Province: Pilbara Craton||||||07-NOV-08
4067|Cistern Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Of the Bookingarra Group. Clastics sediments. Age: 2978Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
4067|Cistern Formation|34829|6|Mentioned|p68|||||||||
4067|Cistern Formation|41073|6|Mentioned|p208|||||||||
4067|Cistern Formation|42231|5|Briefly described|p334|||||||||
4067|Cistern Formation|43769|5|Briefly described|p860|||||||||
4067|Cistern Formation|43821|5|Briefly described|map legend|Archean|Archean|Of Whim Creek Group.||||||07-NOV-08
4067|Cistern Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Age: >.2.9Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
4067|Cistern Formation|63441|3|Fully described|p5 Tb.1, p27|Archean|Archean|Base unit of Croydon Gp.Overlain by Louden and Mount Negri Volcanic Mbrs (Bookingarra Fm) and Kialrah Rhyolite; grades up into Rushall Slate. Age:2964+/-6Ma Geol.prov:Mallina Basin.  With abundant volcaniclastic material from the underlying Whim Creek Gp||||||07-FEB-11
4067|Cistern Formation|63538|4|Described|p7, p6 Fig. 3|Archean|Archean|Of Croydon Group. Overlain by Rushall Slate. Underlain by Whim Creek Group.  Age: 2970 Ma. Geological Province: Pilbara Craton.||||||19-APR-13
4067|Cistern Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup). Age: <2964Ma.  Geological province: Mallina Basin. Siliciclastic and felsic volcaniclastic rocks; metamorphosed.||||||07-NOV-08
4067|Cistern Formation|64580|4|Described|map legend|Mesoarchean|Mesoarchean|Of Croydon Group. Siliciclastic and felsic volcaniclastic rocks; metamorphosed.||||||09-DEC-08
4067|Cistern Formation|65415|4|Described|p119 Fig.1, p121.|Archean|Archean|Miller and Gair (1975). Redefined (Smithies, in prep.). Basal conglomerate is a marker horizon, previously placed in the Mons Cupri Volcanics. The upper part of this unit, and the lower part of the overlying Rushall Slate, host the notable massive sulfide mineralisation within the Whim Creek Belt.||Unit in Whim Creek Group.||Overlies Mons Cupri Volcanics. Is intruded by Opaline Well Complex. Is overlain by the Rushall Slate.|Basal boulder conglomerate; thin arkosic sandstone; welded tuffs, crystal-lithic tuffs, volcaniclastics and clastics in a generally upward-fining sequence; very little lava: several thin basaltic layers.|
4067|Cistern Formation|66217|5|Briefly described|p39, p42.|Mesoarchean|Mesoarchean|Mallina Basin.|c.2964 Ma.|Unit in Croydon Group.|||Quartz-rich clastic sedimentary and felsic volcaniclastic rocks.|
4067|Cistern Formation|67201|4|Described|p7 Fig.4, p12 Tb.1, p21 Fig.12, p23, p57|||In northwestern Pilbara Craton, West Pilbara Superterrane, De Grey Superbasin. In Whim Creek greenstone belt, with direct lithostratigraphic equivalent within southeastern part of Mallina Basin. Minimum depositional age: 2943+/-7 Ma (overlying Kialrah Rhyolite). Cistern Formation and Rushall Slate represent a continuousy upwards-fining siliciclastic sequence with up to 300 m thick sediment.|2964+/-6 Ma (Huston et al. 2002)|Basal unit in Croydon Group (within Whim Creek greenstone belt)||Unconformably overlies rocks of Whim Creek Group. Is overlain gradationally by Rushall Slate.|Basal polymictic conglomerate (clasts derived from underlying Whim Creek Group) and upward-fining succession of subaqueous fanglomerate, breccia, and sandstone.|22-NOV-16
4067|Cistern Formation|69185|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological Province: Pilbara Craton. [Also assigned to Whim Creek Group in 500k_interpgeop_pilcrat02_lut.csv]. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Croydon Group.|||Siliciclastic and felsic volcaniclastic rocks; metamorphosed|
4067|Cistern Formation|69299|5|Briefly described|p6 Tb.1, p7|Archean|Archean|Thickness on COOYA POOYA: 0-800 m. c. 2960 Ma volcanic-hosted massive sulphide Cu-Pb-Zn in Russell Slate and Cistern Formation on SHERLOCK.|<2978 +/- 5 Ma|Of Bookingarra Group.|||Clastic and volcaniclastic rocks, including wacke, sandstone, siltstone, and conglomerate.|
4067|Cistern Formation|69300|5|Briefly described|map legend|Archean|Archean|Mallina Basin, Whim Creek greenstone belt.|<2978 Ma (isotopic age)|Bookingarra Group|||Metamorphosed fine- to medium-grained felsic volcaniclastic rock; local metamorphosed oligomictic conglomerate.|02-SEP-14
4067|Cistern Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p15|||Pilbara Craton. West Pilbara Superterrane. Northwest margin of Mallina Basin.|2960 Ma|Croydon Group||Unconformably overlies Whim Creek Group. Is overlain by Rushalle Slate.|Felsic volcanic rocks. Composed of a basal upward-fining succession of subaqueous fanglomerate, breccia, and sandstone.|
4067|Cistern Formation|70022|6|Mentioned|p115|||West Pilbara Superterrane.||||||
4067|Cistern Formation|70775|4|Described|p12, p41, p44-p46|Mesoarchean|Mesoarchean|Mallina Basin. A maximum depositional age of 2978 Ma is interpreted by Nelson (2000m). Previously interpreted to be equivalent to the Constantine Sandstone (Van Kranendonk et al., 2006) the authors however argue against this [see p45]. Interpreted to be contemporaneous with the VHMS deposits that occur on the flank of the Mons Cupri Dacite Member domes. Also  Conformably overlain by the Rushall Slate. Unconformably overlain by the Louden Volcanics and the Mount Negri Volcanics.  Intruded by the Opaline Well Intrusion. See also p51, p53-p56, p59-p60, p63, p65, p72, p75-p76, p81, p95-p96.|2964 +/- 6 (Huston et al., 2002)|Bookingarra Group||Unconformably overlies the Cattle Well Formation. Unconformably overlies the Red Hill Volcanics.|Volcaniclastic conglomerate, volcanic breccia and various facies of sandstone.|
4067|Cistern Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.|Max age ~2955 Ma, min age 2943+/-7 Ma.|Croydon Group|||Siliciclastic and felsic volcaniclastic rocks; metamorphosed.|
4067|Cistern Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Bookingarra Group.||Overlain by Rushall Slate. Underlain unconformablly by Red Hill Volcanics. Equivalent to Constantine Sandstone.||
4067|Cistern Formation|72668|5|Briefly described|p4, p14, p22|||West Pilbara Superterrane, western Mallina Basin. Contains abundant volcaniclastic material from the Whim Creek Group.|2964 +/- 6 Ma (Huston et al, 2002)|Croydon Group||Overlain by the Rushall Slate. Overlies the Whim Creek Group.|Shows an upward increase in siliciclastic material and parallel decrease in grain size.|12-JAN-22
4103|Clark Sandstone|6943|6|Mentioned|p604.|||Bonaparte Basin. Contains Teriodontus conodonts.||||||
4103|Clark Sandstone|13194|4|Described|p394 Tb. 4-16; p382,399 figs 4-59,-63.|Late Cambrian|Late Cambrian|Type Section: Clark Jump Up 15o27'S 128o38'E. 220-320m thick shallow marine deposits.||Carlton Group||Overlies Pretlove Sandstone or Skewthorp Formation (both conformably).|Red glauconitic feldspathic quartz sandstone.|
4103|Clark Sandstone|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlies Pretlove Sandstone. Overlain by Pander Greensand.||05-OCT-16
4103|Clark Sandstone|24390|5|Briefly described|p2 Fig. 2||Cambrian|Geological Province: Bonaparte Basin.  Of the Carlton Group.||||||
4103|Clark Sandstone|30598|6|Mentioned|p51|||||||||
4103|Clark Sandstone|31572|6|Mentioned|p22|||U.Cambrian. Correlation chart 1.||||||
4103|Clark Sandstone|32109|6|Mentioned|Table 1|||U.Cambrian||||||
4103|Clark Sandstone|32648|6|Mentioned|p32|||U. Camb.||||||
4103|Clark Sandstone|32664|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|Briefly described in notes||||||
4103|Clark Sandstone|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969)||||||
4103|Clark Sandstone|36551|6|Mentioned|Table 16|||||||||
4103|Clark Sandstone|36890|3|Fully described|p375|||||||||
4103|Clark Sandstone|38277|6|Mentioned|p150|||||||||
4103|Clark Sandstone|40136|5|Briefly described|p21|||||||||
4103|Clark Sandstone|41864|3|Fully described|p45|||||||||
4103|Clark Sandstone|42354|6|Mentioned|p9|||Bonaparte Basin||||||
4103|Clark Sandstone|45038|14|Not recorded|p.34||Cambrian|Fig 35,36. p.60,61.||||||
4103|Clark Sandstone|45039|6|Mentioned|Fig.2|||Upper Cambrian.||||||
4103|Clark Sandstone|45053|6|Mentioned|p1|||Refers to Opik in Kaulback & Veevers (1965)||||||
4103|Clark Sandstone|45058|5|Briefly described|p7|||||||||05-OCT-16
4103|Clark Sandstone|45063|6|Mentioned|p6|||Cambrian. See Appendix 2.||||||
4103|Clark Sandstone|45130|6|Mentioned|p15|||||||||
4103|Clark Sandstone|47040|6|Mentioned|Fig.2|||||||||
4103|Clark Sandstone|48886|4|Described|p.47||Late Cambrian|See also Figs & Plates. App.2, p.66,67. Upper Cambrian.||||||
4103|Clark Sandstone|50085|5|Briefly described|p2 Fig. 2|Late Cambrian|Late Cambrian|Of the Carlton Group.  Geological Province: Bonaparte Basin.||||||
4103|Clark Sandstone|60364|6|Mentioned|p185 Fig.2|Late Cambrian|Late Cambrian|||||||
4103|Clark Sandstone|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||11-APR-08
4103|Clark Sandstone|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
4103|Clark Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
4103|Clark Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
4103|Clark Sandstone|69437|5|Briefly described|p22:10|Furongian|Series 3|Bonaparte Basin, Centralian B Superbasin.||Carlton Group.||Overlies Pretlove Sandstone. Is overlain by Pander Greensand.||12-JUL-16
4103|Clark Sandstone|69452|5|Briefly described|p36:5|Furongian|Series 4|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Conformably overlies Pretlove Sandstone. Is overlain conformably by Pander Greensand.||12-JUL-16
4103|Clark Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Carlton Group.||||
4103|Clark Sandstone|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian |||Carlton Group||Overlies Pretlove Sandstone, overlain by Pander Greensand||
4103|Clark Sandstone|71146|5|Briefly described|p6|Cambrian|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Pretlove Sandstone. Overlain by the Pander Greensand.|Sandstone.|
4132|Cleaverville Formation|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3000 Ma||||||07-NOV-08
4132|Cleaverville Formation|22471|5|Briefly described|25|Archean|Archean|Geol province Pilbara||||||07-NOV-08
4132|Cleaverville Formation|22615|6|Mentioned|p 5|||||||||
4132|Cleaverville Formation|22642|6|Mentioned|485|||Geol province Pilbara Craton||||||
4132|Cleaverville Formation|22715|5|Briefly described|table7, p217|Archean|Archean|Age: 3270-3200Ma||||||07-NOV-08
4132|Cleaverville Formation|22727|6|Mentioned|p636,8||Archean|after Hickman 1983||||||07-NOV-08
4132|Cleaverville Formation|23046|5|Briefly described|175|||Overlain by Whim Creek Group, Roebourne Group, Whundo Group.||||||26-JUL-07
4132|Cleaverville Formation|23128|5|Briefly described|p372|||||||||
4132|Cleaverville Formation|23244|5|Briefly described|p14||Archean|Age: 3020-3015Ma. of Gorge Creek Group.||||||07-NOV-08
4132|Cleaverville Formation|23484|4|Described|p10 table 3|Archean|Archean|Of Gorge Creek Group. Maximum thickness: ~1500m.||||||07-NOV-08
4132|Cleaverville Formation|23743|5|Briefly described|p4|Archean|Archean|Overlain by Mons Cupri Volcanics. Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|23783|6|Mentioned|p17|||||||||
4132|Cleaverville Formation|23784|5|Briefly described|p2|Archean|Archean|Age: 3020Ma.||||||07-NOV-08
4132|Cleaverville Formation|23789|4|Described|p11|Archean|Archean|Of the Gorge Creek Group.  Max. thickness: 1500m.  Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|23793|4|Described|p17|Archean|Archean|Age: 3020Ma. Of Gorge Creek Group. Geological Province: Pilbara Craton.||||||22-APR-09
4132|Cleaverville Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|23807|6|Mentioned|p109 Fig. 1|||Geological Province: Pilbara Craton.||||||
4132|Cleaverville Formation|23813|5|Briefly described|p95|Archean|Archean|Banded ironstone/silica-shale formation.  Age: 3016Ma. Geological Province: Pilbara Craton.  See also p90 Tb. 1.||||||07-NOV-08
4132|Cleaverville Formation|23895|5|Briefly described|p885 Fig.2|||Of the Gorge Creek Group.  Geological Province: Pilbara Craton.||||||07-MAR-05
4132|Cleaverville Formation|23936|4|Described|p2, Tb.1, Fig.4|Archean|Archean|Age: ca 3015 Ma. Geological Province: Pilbara Craton. Overlain by De Grey Group (unconformably). Underlain by Whundo Group (unconformably).||||||01-MAR-10
4132|Cleaverville Formation|24023|5|Briefly described|p9 table 2|Archean|Archean|Maximum thickness: 1500m.||||||07-NOV-08
4132|Cleaverville Formation|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton||||||07-NOV-08
4132|Cleaverville Formation|24025|4|Described|p8 Tb. 1, p8|Archean|Archean|Of Gorge Creek Group.  Banded-iron formation, chert, fine-grained clastic sedimentary rocks.  Max. thickness: ~1000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|24166|4|Described|p12|Archean|Archean|Of the Gorge Creek Group.   Age: c.3020Ma.||||||07-NOV-08
4132|Cleaverville Formation|24184|4|Described|p709, p710 Fig.9|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton. Age: ca.3020-3015Ma. Further dating may nessecitate future review of inclusion with Gorge Creek Group||||||07-NOV-08
4132|Cleaverville Formation|24185|5|Briefly described|p737 Tb.2|Archean|Archean|Age: ca. 3020 Ma. Geological Province: Pilbara Craton. Placed in the Gorge Creek Group by Van Kranendonk et al (2002) but it is possible the two were deposited in two intervals (not proven).||||||07-NOV-08
4132|Cleaverville Formation|24189|5|Briefly described|p802 Fig.1|Archean|Archean|Age: >3020 Ma. Geological Province: Mallina basin||||||07-NOV-08
4132|Cleaverville Formation|24190|6|Mentioned|p820 Fig.1|||||||||
4132|Cleaverville Formation|24327|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group.   Age: >3020Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|24349|5|Briefly described|Map legend|Archean|Archean|Of Gorge Creek Group.   Age: 3020Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|24353|4|Described|p5|Archean|Archean|Overlain by Whim Creek Group. Underlain by Whundo Group. Age: c.3020Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|24533|5|Briefly described|p4|Archean|Archean|Of the Gorge Creek Group. Age: c.3015Ma (Smithies et al, 1999).||||||07-NOV-08
4132|Cleaverville Formation|24541|2|Defined|p11 Tb.2, p24-25|Archean|Archean|Of the Gorge Creek Group. Geological Province: Pilbara Craton. Age: c. 3020 Ma. Unconformably overlies the Roebourne Group and Whundo Group. Unconformably overlain by the Fortescue Group. Maximum Thickness: 1500m.||||||23-DEC-09
4132|Cleaverville Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (Pilbara Supergroup).  Age: c.3020Ma.  Banded iron formation, ferruginous chert, jaspilite, chert, siltstone, shale.||||||23-DEC-09
4132|Cleaverville Formation|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Comprises BIF, chert, volcanogenic sediments and minor felsic and mafic volcanics, all metamorphosed to lower greenschist facies. Overlies Regal Formation in West Pilbara. Age: ca 3020-3015Ma. Thickness: 1.5km. See also p41, p74 Tb. 5.1.||||||07-FEB-11
4132|Cleaverville Formation|24554|5|Briefly described|p4|Archean|Archean|Of the Gorge Creek Group. Age: contains chert dated at c. 3015 Ma.||||||07-NOV-08
4132|Cleaverville Formation|24590|6|Mentioned|p28 Fig. 1.2|||Geological Province: Pilbara Craton.||||||07-FEB-11
4132|Cleaverville Formation|30766|6|Mentioned|p5|||||||||
4132|Cleaverville Formation|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
4132|Cleaverville Formation|30882|5|Briefly described|p50|||||||||
4132|Cleaverville Formation|31853|6|Mentioned|p62|||||||||
4132|Cleaverville Formation|36874|5|Briefly described|p87|||||||||
4132|Cleaverville Formation|37373|4|Described|p75|||||||||
4132|Cleaverville Formation|38498|5|Briefly described|Table 1|||||||||
4132|Cleaverville Formation|38544|6|Mentioned|Fig.1|||||||||
4132|Cleaverville Formation|39697|4|Described|p100|||See also p14,18.||||||26-JUL-07
4132|Cleaverville Formation|41073|6|Mentioned|p200|||||||||
4132|Cleaverville Formation|41252|6|Mentioned|p49|||||||||
4132|Cleaverville Formation|41263|6|Mentioned|Fig.1|||||||||
4132|Cleaverville Formation|41352|6|Mentioned|p59|||||||||
4132|Cleaverville Formation|41353|4|Described|p71|||||||||
4132|Cleaverville Formation|41354|6|Mentioned|p92|||||||||
4132|Cleaverville Formation|41355|6|Mentioned|p114|||||||||
4132|Cleaverville Formation|41768|6|Mentioned|p9|||||||||
4132|Cleaverville Formation|42190|6|Mentioned|p272|||||||||
4132|Cleaverville Formation|42231|6|Mentioned|p334|||||||||
4132|Cleaverville Formation|43595|6|Mentioned|p213|||||||||
4132|Cleaverville Formation|43698|6|Mentioned|p26|||||||||
4132|Cleaverville Formation|43779|5|Briefly described|p4-21|||||||||
4132|Cleaverville Formation|44150|5|Briefly described|p129 Tb.2-15, p132 Fig.2-131, p134-135|||See also p152 Tb.2-22, p157 Fig.2-144. Exceptionally thick (1km) BIF. Includes the BIF at Mount Goldsworthy.||Soanesville Subgroup||Equivalent to Paddy Market Formation.|BIF, ferruginous chert, ferruginous shale, tuff.|
4132|Cleaverville Formation|44501|14|Not recorded|p.6, table 2, map||Archean|(ref. to Ryan and Kriewaldt 1964). (F/50-7).. Defn on Tech.File SF/50-3.||||||07-NOV-08
4132|Cleaverville Formation|44502|14|Not recorded|map legend||Archean|||||||07-NOV-08
4132|Cleaverville Formation|44536|14|Not recorded|map legend||Archean|||||||07-NOV-08
4132|Cleaverville Formation|46319|5|Briefly described|p5|Archean|Archean|Of Gorge Creek Group.  Geological Province: Pilbarra Craton.||||||07-NOV-08
4132|Cleaverville Formation|50189|5|Briefly described|p16|Archean|Archean|Thick units of banded iron formation and chert that link the Gorge Creek Group and similar rocks in the Pilbara. Name replaced by Nimingarra Iron Formation in the northwestern part of the Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|50302|5|Briefly described|Map Legend|Archean|Archean|Of the Gorge Creek Group. Chert and banded iron formation.  Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville Formation|50370|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Age: c. 3020 Ma||||||07-NOV-08
4132|Cleaverville Formation|50379|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Age: c. 3020 Ma||||||07-NOV-08
4132|Cleaverville Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Gorge Creek Group. Geological Province: Pilbara Craton. Age: c. 3020 Ma.||||||07-NOV-08
4132|Cleaverville Formation|50430|4|Described|p153||Archean|3020 Ma. Disconformably overlies Regal Formation. Metasedimentary - Banded Iron Formations, ferruginous chert, grey-white and black chert, shale, siltstone and minor volcanogenic sedimentary rocks.||||||07-NOV-08
4132|Cleaverville Formation|60362|5|Briefly described|p1516, p1518 Fig.2|Archean|Archean|Basement to NW Mallina Basin.|3.02-3.015 Ga.||||Cherts and BIF.|
4132|Cleaverville Formation|60429|6|Mentioned|p16|||The part of this unit occurring in NE Pilbara Craton is now renamed as Nimingarra Iron Formation. Comprises BIF, jaspilite, banded and ferruginous chert, black shale and mudstone. Further lithological detail included.||||||07-FEB-11
4132|Cleaverville Formation|61253|5|Briefly described|p53|Archean|Archean|Previously included in Gorge Creek Group but now independent. Age: ~3.02-2.79Ga.   Geological Province: Pilbara Craton. See also p50 Fig. 1, p52 Fig. 2, p58.||||||07-NOV-08
4132|Cleaverville Formation|61267|5|Briefly described|p72 Fig.1|Archean|Archean|Age: c. 3020 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
4132|Cleaverville 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
4132|Cleaverville Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Gorge Creek Group. Geological Province: East Pilbara Granite-Greenstone Terrane. Age <3016Ma. Banded iron formation, jaspilite, chert, siltstone, shale, and minor felsic volcaniclastic rock; metamorphosed.||||||23-DEC-09
4132|Cleaverville Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Gorge Creek Group (De Grey Supergroup).  Age: c. 3020Ma. Geological Province: Pilbara Craton. Chert and banded-iron formation; minor felsic volcaniclastic rock; metamorphosed.||||||07-NOV-08
4132|Cleaverville Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Gorge Creek Group (De Grey Supergroup). Geological Province: Gorge Creek Basin/ Pilbara Craton. Chert and banded iron formation, minor felsic volcaniclastic rock, shale and siltstone; metamorphosed.||||||07-NOV-08
4132|Cleaverville Formation|63441|3|Fully described|p5 Tb.1, p26 |Archean|Archean|Of Gorge Creek Gp. Unconform.on Regal Fm, Warrawoona/Kelly Gps + Muccan Granitic Complex. Age:c.3.02Ga. In Gorge Creek Basin.Comprises BIF, ferruginous chert, grey-white or black chert + metamorphosed shale, siltstone + minor volcanogenic sedimentary rock||||||07-FEB-11
4132|Cleaverville Formation|63518|5|Briefly described|p752|Archean|Archean|Age: 3195+/-15Ma (U-Pb zircon: Kiyokawa et al 2002). Geological Province: Pilbara Craton. Mainly sedimentary rocks.||||||07-NOV-08
4132|Cleaverville Formation|63538|4|Described|p7, p29, p9 Fig. 3, p6 Fig. 3|Archean|Archean|Of Gorge Creek Group. Overlain unconformably by Whim Creek Group, and by Cundaline Formation, underlain by Farrel Quartzite. Age: 3020Ma. Geological Province: Plibara Craton. Sedimentary rocks.||||||08-SEP-15
4132|Cleaverville Formation|64174|5|Briefly described|Map legend|Archean|Archean|Of Gorge Creek Group (De Grey Supergroup). Geol.prov: Gorge Creek Basin, Pilbara Craton. Chert and banded-iron formation, minor felsic volcaniclastic rock; metamorphosed.||||||07-NOV-08
4132|Cleaverville Formation|64328|5|Briefly described|p56 Tb. 1|||||||||07-FEB-11
4132|Cleaverville Formation|64384|5|Briefly described|p26 Tb. 3|Archean|Archean|Of the Gorge Creek Group. Max. thickness: 1km.||||||07-FEB-11
4132|Cleaverville Formation|64580|4|Described|map legend||Mesoarchean|Of Gorge Creek Group. Chert and banded iron-formation, felsic volcaniclastic rock, volcanolithic sandstone, and siltstone; metamorphosed.||||||09-DEC-08
4132|Cleaverville Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of Croydon Group (De Grey Supergroup).Chert and minor jaspillite; BIF and ferruginous chert; black shale with minor chert and BIF, local siltstone; layered chert derived from shale, minor silicified sandstone.||||||07-NOV-08
4132|Cleaverville Formation|64632|5|Briefly described|p203|Mesoarchean|Mesoarchean||3020 Ma|Of the Gorge Creek Group.|||Clastic sedimentary rocks, felsic tuffs and porphyries, and banded iron formation.|
4132|Cleaverville Formation|64688|5|Briefly described|Map legend|Archaean|Archaean|Geological province: Pilbara Craton. Banded iron formation hosting supergene-enriched hematite and hematite-goethite mineralisation.||||||
4132|Cleaverville Formation|65727|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, Pilbara Craton.||Of Gorge Creek Group.||Overlies Farrel Quartzite.|Chert and banded iron-formation; minor felsic volcaniclastic rock; metamorphosed.|
4132|Cleaverville Formation|65827|3|Fully described|p6 Tb.1, p16, p29, p33, p41, p48|Mesoarchean|Mesoarchean|Of Gorge Creek Group (De Grey Supergroup). Overlies Farrel Quartzite; unconformably underlies Mount Roe Basalt, Hardey Formation; faulted against Apex Basalt, Zulu Granodiorite. Banded iron-formation and ferruginous chert.||||||
4132|Cleaverville Formation|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit in Gorge Creek Group. Banded iron-formation, ferruginous chert, sandstone, siltstone and shale; minor grey-white chert and felsic volcaniclastic rock; metamorphosed.||||||
4132|Cleaverville Formation|66118|5|Briefly described|p151, p158, p160|||Pilbara Craton. West Pilbara Superterrane. Regal Terrane.|3020 Ma|De Grey Supergroup||Stratigraphically overlies Cleaverville Formation.||
4132|Cleaverville Formation|66122|5|Briefly described|p73-78, 84-85 Fig.9, p86|Archean|Archean|Mount Goldsworthy greenstone belt, NE Pilbara Craton. Fining (deepening)-upward sequence. Simplified stratigraphic column. Chemical analyses of chert samples for REE and Y tabulated and discussed.||Gorge Creek Group.||Conformably overlies Farrel Quartzite.|Includes black shale, siltstone, and laminated to banded chert including carbonaceous chert, jaspilite and BIF.|
4132|Cleaverville Formation|66217|4|Described|p9, p39, pp40-41.|Mesoarchean|Mesoarchean|East Pilbara Terrane, Pilbara Craton. See also reference to (mis-spelled) Clearville Formation (p5). Type area at Cleaverville Beach. Extends across the whole of the exposed Pilbara Craton. Up to 1900 m thick. Formerly, parts of this unit were assigned to Nimingarra Iron-Formation or Paddy Market Formation of the Gorge Creek Group.|3.02 Ga.|Upper unit in Gorge Creek Group.||Conformably overlies Farrel Quartzite.|Widespread unit of banded iron-formation, also shale and felsic volcaniclastic rocks; minor siltstone and sandstone.|
4132|Cleaverville Formation|67130|6|Mentioned|p61|Mesoarchean|Mesoarchean||c. 3000 Ma|De Grey Supergroup|||Banded iron Formation|
4132|Cleaverville Formation|67197|5|Briefly described|p9, p14, p19, p22, p29, p33-34, p36, p38|||Shown on the legend, but not the map, on p9.||Gorge Creek Group.||Unconformably overlies Strelley Pool Formation.|Shale, chert and sandstone.|
4132|Cleaverville Formation|67201|4|Described|p7, p12, p15-17, p20-21, see comments|||In northwestern Pilbara Craton, West Pilbara Superterrane and East Pilbara Terrane, De Grey Superbasin, Gorge Creek Basin. Depositional environment: shallow-marine and continental. SHRIMP, U-Pb zircon, volcanogenic sedimentary rocks; max. depositional age between 3022 Ma (GSWA 127330: Nelson 1998a) and 3018 Ma (GSWA 142830: Nelson 1998h); min age indicated by felsic intrusions dated 3015 Ma (GSWA 136899; Nelson 1998d) and 3014 Ma (GSWA 127320: Nelson 1997d). c. 3020 Ma. Related units continued: Is unconformably overlain by Warambie Basalt. Where Mount Roe Basalt is absent, Hardey Formation unconformably rests on irregular paleosurface composed of Whundo Group, Cleaverville Formation, and Whim Creek Group. Page location continued: p23-25, p27, p49, p68-69.||Central unit in Gorge Creek Group in east Pilbara; only unit in Gorge Creek Group in west Pilbara||In west Pilbara, overlies Regal Formation and informal "Sixty-six Hills Member". Is disconformably overlain by Cundaline Formation in northeast Pilbara. Intruded by Orpheus Supersuite. See comments|Chert and banded-iron formation; minor felsic volcaniclastic rocks; chert interbedded with shale, mudstone, and tuff; metamorphosed.|
4132|Cleaverville Formation|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Gorge Creek Group.|||BIF.|
4132|Cleaverville Formation|68035|5|Briefly described|p290, 293|Mesoarchean|Mesoarchean|Gorge Creek Basin. 1000 m thick. Includes carbonaceous spheroids in black chert.||Gorge Creek Group|||BIF, chert, and black shale|
4132|Cleaverville Formation|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin, Pilbara Craton.|3022-3016 Ma|Of the Gorge Creek Group.|||Banded iron formation, chert, sandstone, siltstone, and minor felsic volcaniclastic rock; metamorphosed.|
4132|Cleaverville Formation|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin. Age inferred from age of parent unit. The 4 facies are mapped separately.|c.3020 Ma|Of the Gorge Creek Group.|||Chert and banded iron-formation, minor felsic volcaniclastic rock, shale, and siltstone; white and grey chert, minor jaspilite, ferruginous chert; banded iron-formation, local banded quartz-magnetite-grunerite rock; shale; all metamorphosed.|07-JAN-15
4132|Cleaverville Formation|68284|5|Briefly described|p7|Archean|Archean|Kelly greenstone belt, East Pilbara Terrane.|c.3020 Ma.|||Overlies Farrel Quartzite.||
4132|Cleaverville Formation|68574|4|Described|iv, p1, p3-7, p9-11, p14|Mesoarchean|Mesoarchean|Ryan and Kriewaldt (1964). Cleaverville Beach area, NW Pilbara Craton. Thickness over 300m. Contains carbonaceous coccoid-like microstructures resembling cyanobacterial microfossils. Affected by low-grade metamorphism (prehnite-pumpellyite facies); no intensive deformation.  U-Pb age from a large spread of zircon ages (c.3700-3100 Ma); other age determinations given.|3108 +14/-7 Ma (Aihara et al., 2012).|||Overlies Regal Formation, Port Robinson Basalt.|Crops out as red to pink shale (weathered black shale), bedded reddish-white chert (silicified shale units) and BIF (part of which may represent silicified shale). Local pyroclastic beds contain chert fragments.|
4132|Cleaverville Formation|69012|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin.|3022-3016 Ma|Of the Gorge Creek Group.|||Banded iron-formation and ferruginous chert, local banded quartz-magnetite-grunerite rock, metamorphosed; ferruginous shale, metamorphosed.|29-APR-14
4132|Cleaverville Formation|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin. Age constrained by the De Grey Supergroup.|3022-3016 Ma|Of the Gorge Creek Group.|||Banded iron-formation, ferruginous chert, sandstone, siltstone and shale; minor grey-white chert and felsic volcaniclastic rock; metamorphosed.|30-APR-14
4132|Cleaverville Formation|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Gorge Creek Basin, De Grey Superbasin. Mapped as 2 unnamed sub-units.|3022-3016 Ma|Of the Gorge Creek Group.|||Banded iron-formation and ferruginous chert, local banded quartz-magnetite-grunerite rock; black shale, with minor chert and banded iron-formation, local siltstone; all metamorphosed.|02-MAY-14
4132|Cleaverville Formation|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Gorge Creek Group|||Banded iron-formation, ferruginous chert, sandstone, siltstone and shale. Metachert and banded iron formation. Siliciclastic sedimentary ocks; pebble and cobble conglomerate and breccia.Pebbly sandstone and lithic arenite; fine-medium grained wacke.|
4132|Cleaverville Formation|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological province: West And East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 3020 Ma|Unit of Gorge Creek Group.|||Felsic volcaniclastic rock, volcanolithic sandstone, and siltstone; metamorphosed; chert and banded iron-formation; metamorphosed.|
4132|Cleaverville Formation|69300|5|Briefly described|map legend|Archean|Archean|West Pilbara Granite-Greenstone Terrane; and East Pilbara Granite-Greenstone Terrane. Isotopic ages: Older detrital populations ages, c.3058 Ma, c.3070, c.3110, c.3170, Nelson 1998; shown on legend as 3020-3015 Ma.|<3022 Ma,Nelson 1998; <3016 Ma,Nelson, 1998and2001|Gorge Creek Group|||Banded iron-formation, jaspilite, chert, siltstone, shale, and minor felsic volcaniclastic rock|02-SEP-14
4132|Cleaverville Formation|69301|4|Described|p5 Fig.3, p9 Tb.1, p14-15, p20 Tb.2, p22|||Pilbara Craton. West Pilbara Superterrane and East Pilbara Terrane. Gorge Creek Basin.|3020 Ma|Central unit of Gorge Creek Group||Is overlain by Cundaline Formation. Overlies Farrel Quartzite.|Sedimentary rocks. Chert, BIF, carbonaceous shale, and local siltstone and sandstone. Carbonaceous spheroids in black chert could be microfossils.|
4132|Cleaverville Formation|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Gorge Creek Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeol_lut.csv.|3022-3016 Ma (isotopic and inferred)|Unit of Gorge Creek Group.|||Banded iron-formation, chert; banded, grey and white, can be ferruginous, metamorphosed; black shale, metamorphosed wacke interlayered with schist and meta iron-formation, sandstone, lithic arenite, siltstone.|
4132|Cleaverville Formation|70022|6|Mentioned|p115|||Pilbara Craton.||Gorge Creek Group.||||
4132|Cleaverville Formation|70775|3|Fully described|iv, p10-p12, p15-p16, p24 tbl 3|Mesoarchean|Mesoarchean|Gorge Creek Basin. An approximate depositional age on the western margin of the Eastern Pilbara Terrain is c. 3016 Ma (SHRIMP U-Pb, Nelson, 1998o); detrital zircons in the sandstone from which this date is derived are from the Elizabeth Hill Supersuite, the Soanesville Group or the Nickol River Formation. This unit has a type area at Cleaverville Beach where it is exceptionally well exposed. This unit is up to 1500m thick at the type area. Lithology at the type area is briefly discussed. This unit has been correlated with BIF and chert that immediately underlies the Constantine Sandstone in the central part of the Mallina Basin. This formation is the primary source of iron ore in the Pilbara and additionally hosts minor gold deposits. This formation is overlain by the Cundaline Formation, Whim Creek Group and the Croydon Group.  Unconformably overlain by the Warambie Basalt. Intruded by the Stone Yard Granophyre and the Orpheus Supersuite. See also p29-p30, p38-p39, p41, p43, p46-p50, p52, p55-p57, p62, p69-p70, p73-p74, p78.|c. 3022-3015 Ma|Gorge Creek Group||Unconformably overlies the Regal Formation and the Whundo Group. Overlies the  Farrel Quartzite.|Chert, banded iron formation, carbonaceous shale, siltstone and sandstone; minor felsic volcaniclastic rock; metamorphosed.|
4132|Cleaverville Formation|71041|4|Described|p41, p43-p47, p55-p57, p59, p60|Mesoarchean|Mesoarchean|De Grey Superbasin. Hosts several high grade (more than 50 percent weight iron) iron ore deposits which are currently being mined. At least 600m thick in the Wodgina greenstone belt.  |3020 Ma|Gorge Creek Group||Unconformably overlies the Honeyeater Basalt. Overlain by the Mallina Formation.|Quartzite, banded iron formation, shale and siltstone turbidite deposits.|
4132|Cleaverville Formation|71136|6|Mentioned|p267|||Pilbara Craton.||||Overlies Farrel Quartzite.||
4132|Cleaverville Formation|71137|5|Briefly described|p2-5, 12|Archean|Archean|Mount Grant area, Pilbara Craton. Shallow sea or lake deposits. Metamorphic history varies from west to east Pilbara. Up to 1000m thick. MDA of 3058 +/- 7 Ma (SHRIMP: Nelson, 1998) from near-basal volcanic sandstone layer.||Gorge Creek Group.||Conformably overlies Farrel Quartzite.|Laminated shale and BIF, interbedded with pillow basalts (western Pilbara Craton) and submarine fan facies turbidites (southern Pilbara block).|
4132|Cleaverville Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Gorge Creek Basin.|Max age 3022+/-12 Ma, min 2016+/-13 Ma.|Gorge Creek Group|||Banded iron-formation, ferruginous chert, sandstone, siltstone and shale; minor grey-white chert and felsic volcaniclastic rock; metamorphosed.|
4132|Cleaverville Formation|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton.||Unit of Gorge Creek Group.||Overlain by Cundaline Formation, or unconformably by Waramie Basalt or Constantine Sandstone. Underlain by Farrel Quartzite, or unconformably by Woodbrook or Nallana formations.||
4132|Cleaverville Formation|72668|4|Described|p4, p13-15, p21-22, p28-29|||West Pilbara Superterrane and East Pilbara. Occurs on both sides of the SSZ providing a maximum time of juxtaposition between the Karratha and Sholl Terranes. Crops out within antiformal culminations within the Mallina Basin along the Eastern margin of the basin. Felsic tuff dated at c. 3195 Ma by Kiyokawa et al, 2002 and represents the maximum age of the tuff. Detrital zircon populations characteristic of East Pilbara (Warrawoona Group/Callina and Tambina Supersuites), Karratha Terrane ( Sulphur Springs Group/Cleland Supersuite) and West Pilbara Superterrane (Whundo Group, Elizabeth Hill Supersuite). Mentioned as Cleaverville Group, immature island arc, p2.|c. 3020-3015 Ma (depositional age)|Gorge Creek Group||Overlies the Farrel Quartzite. Overlain by the Cundaline Formation.|Volcaniclastic rocks including felsic tuff. Banded iron formation.|12-JAN-22
4132|Cleaverville Formation|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||Gorge Creek Group.||Overlies Farrel Quartzite. Is overlain by Cundaline Formation.||
4221|Coates Gabbro|35726|6|Mentioned|p97|||||||||
4221|Coates Gabbro|40903|6|Mentioned|p45|||||||||
4221|Coates Gabbro|41594|4|Described|p66|||||||||
4273|Cockatoo Group|13194|4|Described|p392 Tb. 4-16; p382,402 figs 4-59,-66|Frasnian|Frasnian|1600-2700m thick continental to shallow marine rocks probably equivalent to Bonaparte Formation.||||Overlies Carlton Group or Antrim Plateau Volcanics (both unconformably).||
4273|Cockatoo Group|13234|6|Mentioned|p252 Fig.4,p260 Tb.1, |||Clastics in thie unit are a potential reservoir.||||||
4273|Cockatoo Group|14228|5|Briefly described|p6 fig3|Devonian|Devonian|Southern Bonaparte Basin.||||Overlain by Ningbing Group.||05-OCT-16
4273|Cockatoo Group|22547|5|Briefly described|p30||Late Devonian|Geological province: Bonaparte Basin.||||||14-NOV-06
4273|Cockatoo Group|22663|5|Briefly described|W97 8 to 10 fig.3||Devonian|||||||01-MAR-10
4273|Cockatoo Group|22814|5|Briefly described|fig2|Late Devonian|Late Devonian|||||||
4273|Cockatoo Group|23377|6|Mentioned|p212 Fig.5||Devonian|Of Vulcan Sub-basin.||||||07-AUG-06
4273|Cockatoo Group|23858|5|Briefly described|p919|||Geological Province: Bonaparte Basin. Max. thickness: 2700 m.||||||
4273|Cockatoo Group|24390|5|Briefly described|p2 Fig. 2|Late Devonian|Devonian|Geological Province: Bonaparte Basin.||||||
4273|Cockatoo Group|24503|5|Briefly described|Map legend|Devonian|Devonian|Sandstone, conglomerate, and limestone; minor dolomite and siltstone.  Geological Province: Bonaparte Basin.||||||
4273|Cockatoo Group|24569|5|Briefly described|p248 Fig. 3|Late Devonian|Late Devonian|Geological Province: Petrel Sub-basin.||||||
4273|Cockatoo Group|40792|6|Mentioned|p175|||||||||
4273|Cockatoo Group|40993|3|Fully described|p3|||First named Cockatoo Series, then Cockatoo Sandstone later Cockatoo Fm.||||||09-DEC-08
4273|Cockatoo Group|41459|6|Mentioned|Fig.2|||||||||
4273|Cockatoo Group|41532|6|Mentioned|p292|||||||||
4273|Cockatoo Group|41598|6|Mentioned|p412|||||||||
4273|Cockatoo Group|41731|5|Briefly described|p578|||See also p574.||||||07-AUG-06
4273|Cockatoo Group|41864|4|Described|p47|||Formerly Cockatoo "Formation" "Cockatoo Series", "Cockatoo Sandstone"||||||
4273|Cockatoo Group|41865|6|Mentioned|Map legend|Frasnian||||||||
4273|Cockatoo Group|41867|6|Mentioned|Map legend|Frasnian||||||||
4273|Cockatoo Group|42030|5|Briefly described|p748|||||||||
4273|Cockatoo Group|42442|5|Briefly described|Fig.6 P9|||Variation of Cockatoo Group, WA.||||||
4273|Cockatoo Group|42933|5|Briefly described|Fig.94 p258|||||||||
4273|Cockatoo Group|43236|5|Briefly described|Fig.13, p13|Late Devonian||Bonaparte Basin.||||||
4273|Cockatoo Group|43661|6|Mentioned|Fig.3|||||||||
4273|Cockatoo Group|43853|5|Briefly described|Map Legend||Frasnian|||||||
4273|Cockatoo Group|44230|5|Briefly described|Map Legend|Frasnian|Frasnian|||||||26-JUL-06
4273|Cockatoo Group|50085|5|Briefly described|p2 Fig. 2|Devonian|Devonian|Geological Province: Bonaparte Basin.||||||
4273|Cockatoo Group|60006|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin. Includes: Kellys Knob Sandstone, Ragged Range Conglomerate. Sandstone, conglomerate.||||||23-JUL-04
4273|Cockatoo Group|60364|6|Mentioned|p186 Fig.3|||||||||
4273|Cockatoo Group|60682|4|Described|piii, 23|Permian|Devonian|Contains 10 formations. Coarse grained clastics. Alluvial fan deposits. Previously Cockatoo Formation. Unconformaly overlain by Ninbing Group. Geological Province: Bonaparte Basin.||||||
4273|Cockatoo Group|61023|5|Briefly described|p2 Fig. 2|Devonian|Devonian|Geological Province: Bonaparte Basin.||||||11-APR-08
4273|Cockatoo Group|61542|6|Mentioned|p278, p281 Fig. 7|Devonian|Devonian|||||||07-FEB-11
4273|Cockatoo Group|64580|4|Described|map legend||Late Devonian|Sandstone, conglomerate, and limestone; minor dolomite and siltstone; includes STEEPLE PEAK, KELLYS KNOB, CYRIL, ABNEY, MAUDOBAR and CECIL SANDSTONES, KUNUNURRA, GALLOPING CREEK, and HARGREAVES FORMATIONS, and RAGGED RANGE CONGLOMERATE.||||||09-DEC-08
4273|Cockatoo Group|64694|5|Briefly described|Fig.5, p249, p253|Frasnian |Frasnian |||||Is overlain unconformably by Buttons Formation.||
4273|Cockatoo Group|65331|5|Briefly described|Map legend + overview geology map legend|Late Devonian|Late Devonian|Of Bonaparte Basin. Includes Kellys Knob Sandstone, Ragged Range Conglomerate. Sandstone, conglomerate||||||
4273|Cockatoo Group|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes ?grey quartzite.|
4273|Cockatoo Group|67200|6|Mentioned|app 2 p8||||||||Quartzite.|
4273|Cockatoo Group|67860|6|Mentioned|p418 Tb.4-18|Frasnian|Frasnian|Of Bonaparte Basin.||||||
4273|Cockatoo Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Late Devonian|Late Devonian|Southern Bonaparte Basin|||Includes Galloping Creek Formation||Sandstone, conglomerate, and limestone; minor dolostone and siltstone|30-JUL-15
4273|Cockatoo Group|69165|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Also includes Kellys Knob Sandstone, Cyril Sandstone, Abney Sandstone, Maudobar Sandstone, Cecil Sandstone, Kununurra Formation, Hargreaves Formation, Ragged Range Conglomerate. See also 500k_geologyp08_lut.csv. |||Includes Galloping Creek Formation, Steeple Peak Sandstone||Undivided; sandstone, conglomerate and limestone; minor dolomite and siltstone|
4273|Cockatoo Group|69422|6|Mentioned|p7:2 Fig.7.2|Devonian|Devonian|Bonaparte Basin.||||||12-JUL-16
4273|Cockatoo Group|69452|4|Described|p36:4-7, 9-11, 13, 15|Frasnian|Frasnian|Rowley and Lee (1986). Petrel Sub-basin, Bonaparte Basin. Up to 2730m thick. Divided into 10 Formations (summarised by Mory and Beere, 1988); only 2 recognised in NT (Dunster et al., 2000). These have complex lateral and vertical stratigraphic relationships, and several unconformities are recognised within the succession.|||(WA): Steeple Peak, Cyril, Abney, Cecil, Maudoobar Sandstones; Kununurra, Galloping Creek, Hargreaves Formations. (WA and NT): Ragged Range Conglomerate, Kellys Knob Sandstone.|Unconformably overlies Antrim Plateau Volcanics and Carlton Group. Is overlain by Ningbing Group conformably or disconformably.|Coarse clastic rocks of E and W faulted Basin margins grade basinward into marine siliciclastic rocks, including siltstone and shale with interbedded sandstone and sandy limestone. Interbeds of dolostone, marl and limestone along W margin.|12-JUL-16
4273|Cockatoo Group|69634|4|Described|GEOL_LUT_CSV files|Late Devonian|Late Devonian|Geological province: Halls Creek Orogen. Of Southern Bonaparte Basin. Events: Alice Springs Orogeny; Mount Eclipse Movement; Pertnjara-Brewer Movements. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|382.7-358.9 Ma (inferred)||Includes SANDSTONE: Steeple Peak, Kellys Knob, Cyril, Abney, Maudobar, Cecil; FORMATION: Kununurra, Galloping Creek, Hargreaves; Ragged Range Conglomerate.||Undivided; sandstone, conglomerate, and limestone; minor dolomite and siltstone|
4273|Cockatoo Group|69653|6|Mentioned|p10, 14|Late Devonian|Late Devonian|Petrel Sub-basin. Shallow-marine to non-marine settings.||||Is overlain by Ningbing Group.|Fine-grained clastic and carbonate sediments.|
4273|Cockatoo Group|69673|5|Briefly described|p168 fig 139, p169, p179, p185, p186|Devonian|Devonian||||Includes Ragged Range Conglomerate, Kellys Knob Sandstone||Arkosic sandstone and carbonate rocks.|
4273|Cockatoo Group|70061|6|Mentioned|Petrel Sub-basin Fig.3|Devonian|Devonian|See also Regional geology: Fig.8, p13, p16. An equivalent unit in the Petrel Sub-basin includes the lower (Frasnian) part of the Bonaparte Formation.||||||12-JUL-16
4273|Cockatoo Group|70154|6|Mentioned|100k_interpgeop_lut.csv|||See also 500k_interpgeop_lut.csv.|||Galloping Creek Formation|||
4273|Cockatoo Group|70206|5|Briefly described|Map Legend|Devonian|Devonian|Bonaparte Basin.|||Includes Kellys Knob Sandstone, Ragged Range Conglomerate.||Sandstone, conglomerate.|
4273|Cockatoo Group|70731|6|Mentioned|p273|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. ||||||
4273|Cockatoo Group|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Southern Bonaparte Basin.||||||
4273|Cockatoo Group|70851|5|Briefly described|p11, p17-p19, p34|||Rock properties are provided.||||||
4273|Cockatoo Group|71146|5|Briefly described|p6|Frasnian|Eifelian|Bonaparte Basin.||||Overlain by the Ningbing Group.|Sandstone.|
4273|Cockatoo Group|71267|4|Described|GEOL_LUT_CSV files|Late Devonian|Late Devonian|Geological Province: Halls Creek Orogen. Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|382.7-358.9 Ma (inferred)||Includes Galloping Creek Formation, Kellys Knob Sandstone.||Quartz sandstone, conglomerate and limestone; minor dolomite and siltstone.|
4273|Cockatoo Group|72034|5|Briefly described|500k_interpgeop16_lut|Late Devonian|Late Devonian|Southern Bonaparte Basin.|||||Sandstone, conglomerate, and limestone; minor dolostone and siltstone.|
4280|Cockburn Sandstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4280|Cockburn Sandstone|32660|5|Briefly described|Table 3|||||||||
4280|Cockburn Sandstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
4280|Cockburn Sandstone|32728|6|Mentioned|Table 5|||||||||
4280|Cockburn Sandstone|36551|6|Mentioned|Table 10|||||||||
4280|Cockburn Sandstone|36885|4|Described|p185|||||||||
4280|Cockburn Sandstone|41811|6|Mentioned|p212|||||||||
4280|Cockburn Sandstone|42821|5|Briefly described|p7|||||||||
4280|Cockburn Sandstone|44140|5|Briefly described|p294|Paleoproterozoic|Paleoproterozoic|More than 500 m thick. ||Bastion Group|||Quartz sandstone; minor micaceous sandstone, shale; cross-beds, ripple marks.|07-MAR-18
4280|Cockburn Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
4280|Cockburn Sandstone|44363|14|Not recorded|p.12|||(Carpentarian) Bastion Group.||||||
4280|Cockburn Sandstone|44364|14|Not recorded|map legend|||Unit of Bastion Group.||||||
4280|Cockburn Sandstone|45047|5|Briefly described|p28|||Bastion Group||||||
4280|Cockburn Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Bastion Group.|||Quartz sandstone, micaceous fine-grained sandstone, shale|
4341|Collett Siltstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4341|Collett Siltstone|32660|5|Briefly described|Table 3|||||||||
4341|Collett Siltstone|32728|6|Mentioned|Table 5|||||||||
4341|Collett Siltstone|36551|6|Mentioned|Table 10|||||||||
4341|Collett Siltstone|36885|4|Described|p184|||||||||
4341|Collett Siltstone|44140|5|Briefly described|p294|Paleoproterozoic|Paleoproterozoic|60 m thick.||Crowhurst Group||Conformably overlies Liga Shale. Is overlain conformably by Hibberson Dolomite.|Laminated purple and green siltstone with minor dolomite interbeds and lenses.|07-MAR-18
4341|Collett Siltstone|44231|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Crowhurst Group. Purple and green siltstone; minor white, silty dolomite, and pyritic cherty siltstone.  Geological Province: Crowhurst Basin.||||||26-MAY-05
4341|Collett Siltstone|44397|14|Not recorded|p.9, Table 2||Carpentarian|Crowhurst Group.||||||
4341|Collett Siltstone|44398|14|Not recorded|map legend||Carpentarian|||||||
4341|Collett Siltstone|45047|5|Briefly described|p28|||Crowhurst Group.||||||
4341|Collett Siltstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Crowhurst Group.|||Purple and green fissile laminated siltstone with minor white and purple silty dolomite interbeds, lenses and nodules; white sandy dolomite and dolomitic sandstone, purple siltstone and dolomitic siltstone, and green pyritic cherty siltstone|
4345|Collie Group|14227|6|Mentioned|Enclos. 2|||Presented as L. Collie Group.||||||07-FEB-11
4345|Collie Group|22820|5|Briefly described|p10 Fig.4|Late Permian|Late Permian|Includes Moorhead Formation, Westralia Sandstone, Ewington C.M., Allanson Sandstone, Premier and Muja Coal Measures.||||||12-AUG-08
4345|Collie Group|23174|5|Briefly described|Fig5p8|||||||||
4345|Collie Group|42711|2|Defined|p5 Fig. 4, p20, Plates 2, 4, 5|Early Permian|Early Permian|Comprises Premier and Muja Coal Measures, Allanson Sandstone, Ewington C.M., and Westralia Sandstone. Conformable on Stockton Group; unconformable below Nakina Fm. Thickness: ~900m. Geological province: Collie Basin. Nomenclatural history presented (p17).||||||11-AUG-08
4345|Collie Group|64580|4|Described|map legend|Late Permian|Early Permian|Sandstone, carbonaceous shale, coal, pebble conglomerate; includes EWINGTON, PREMIER and MUJA COAL MEASURES; sandstone with interbedded subordinate siltstone in coarsening-upward sequence; includes WESTRALIA and ALLANSON SANDSTONES.||||||09-DEC-08
4345|Collie Group|70097|5|Briefly described|p19 Fig.3|Roadian|Sakmarian|Southern Perth Basin. Collie Sub-basin.|||Westralia Sandstone, Ewington Coal Measures, Allanson Sandstone, Premier Coal Measures|Overlies Stockton Group. Is overlain by Muja Coal Measures.||12-SEP-17
4345|Collie Group|70826|6|Mentioned|p6 tbl 3, p11|Early Permian|Late Carboniferous|Collie, Wilga and Boyup Sub-basins of the Perth Basin.||||||20-MAY-20
4345|Collie Group|71146|5|Briefly described|p39|Wordian|Sakmarian|Collie Sub-basin. Up to 900m thick this glaciodeltaic succession hosts up to 60 coal seams up to 13m thick.|||||Coal seams.|
4345|Collie Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone, claystone, conglomerate|
4345|Collie Group|72034|5|Briefly described|500k_interpgeop16_lut|Guadalupian|Sakmarian|Perth Basin.  Age from biostratigraphy.|||Includes Muja Coal Measures, Premier Coal Measures, Allanson Sandstone, Ewington Coal Measures, Westralia Sandstone.||Sandstone, carbonaceous shale, coal, pebble conglomerate.|
4364|Colombo Sandstone|22716|6|Mentioned|table4, p239|Cryogenian|Cryogenian|Age: 830 Ma. Thought to be part of supersequence 1 of Centralian Superbasin||||||
4364|Colombo Sandstone|23383|6|Mentioned|p20|||Unconformably overlain by Louisa Downs Group on MOUNT RAMSAY.||||||25-JAN-05
4364|Colombo Sandstone|23599|6|Mentioned|p16|||||||||
4364|Colombo Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
4364|Colombo Sandstone|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4364|Colombo Sandstone|32660|5|Briefly described|Table 6|||||||||
4364|Colombo Sandstone|32728|5|Briefly described|p40|||||||||
4364|Colombo Sandstone|36551|6|Mentioned|Table 12|||||||||
4364|Colombo Sandstone|36885|4|Described|p177|||||||||
4364|Colombo Sandstone|37462|4|Described|Table 4.V|||||||||
4364|Colombo Sandstone|43281|5|Briefly described|Map legend||Proterozoic|||||||
4364|Colombo Sandstone|44140|5|Briefly described|p293-294, p296 fig 4-3, p299|Mesoproterozoic|Mesoproterozoic|Locally restricted. More than 100 m thick.||||Overlies Crowhurst and Kimberley Groups unconformably. Has been correlated with Mount Parker Sandstone (Birrindudu Basin).|Quartz sandstone, chert-pebble breccia.|07-MAR-18
4364|Colombo Sandstone|44155|6|Mentioned|p251, p254 Fig.3-40|||Part of Kimberley Basin succession.||||||
4364|Colombo Sandstone|44231|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Massive, medium-grained quartz sandstone, and sandy chert-pebble breccia. Age: c.?800Ma.||||||26-MAY-05
4364|Colombo Sandstone|44397|14|Not recorded|p.9,19, Table 2|||Adelaidean or Carpentarian.||||||
4364|Colombo Sandstone|44398|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
4364|Colombo Sandstone|45047|2|Defined|p77|early Adelaidean|late Carpentarian|Early Adelaidean or Late Carpentarian||||||
4364|Colombo Sandstone|60724|6|Mentioned|p5 Fig. 2|||||||||
4364|Colombo Sandstone|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Sandstone and pebble breccia.||||||09-DEC-08
4364|Colombo Sandstone|68244|6|Mentioned|p666|Neoproterozoic|Neoproterozoic|||||Overlain unconformably by Louisa Downs Group.||
4364|Colombo Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Sandstone and pebble breccia.|30-JUL-15
4364|Colombo Sandstone|69165|4|Described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Sandstone and pebble breccia.|
4364|Colombo Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic||||||Sandstone and pebble breccia|
4364|Colombo Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Neoproterozoic||541-1000 Ma||||Sandstone and pebble breccia|29-AUG-18
4364|Colombo Sandstone|71267|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Geological Province: Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1000-541 Ma (inferred)||||Massive medium grained white and purple quartz sandstone and sandy purple chert-pebble breccia|
4364|Colombo Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Halls Creek Orogen.|||||Sandstone and pebble breccia.|
4380|Colville Sandstone|22613|6|Mentioned|p21|||||||||
4380|Colville Sandstone|23768|5|Briefly described|p28 Fig.5, p73|Balcombian|Balcombian|Geological Province: Eucla Basin. See also p113.||||||11-SEP-09
4380|Colville Sandstone|24057|5|Briefly described|p97|Tertiary|Tertiary|Geological Basin: Eucla Basin.||||||
4380|Colville Sandstone|24347|5|Briefly described|p114|||||||||
4380|Colville Sandstone|30012|6|Mentioned|p20|||||||||
4380|Colville Sandstone|30268|6|Mentioned|p44|||||||||
4380|Colville Sandstone|30922|6|Mentioned|Map legend|Miocene|Miocene|||||||
4380|Colville Sandstone|30952|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
4380|Colville Sandstone|30967|6|Mentioned|Map legend|early Miocene|early Miocene|||||||
4380|Colville Sandstone|30974|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|31562|5|Briefly described|p13|||See also p10.||||||02-JUL-08
4380|Colville Sandstone|31636|6|Mentioned|p10|||||||||
4380|Colville Sandstone|31850|4|Described|p38|||Definition summary||||||
4380|Colville Sandstone|31902|4|Described|Table 1|||Lower  Miocene. Fig.1||||||02-JUL-08
4380|Colville Sandstone|31904|5|Briefly described|p8|||equiv. to gradation of Nullarbor limestone.||||||
4380|Colville Sandstone|31906|4|Described|p8|||Refers Lowry (1968). Table 1||||||
4380|Colville Sandstone|31914|6|Mentioned|p99|||Plate 10||||||
4380|Colville Sandstone|31915|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|32552|2|Defined|p10|early Miocene|early Miocene|See also p12, 36, 37, 40 etc.||||||02-JUL-08
4380|Colville Sandstone|32648|6|Mentioned|p32|||Miocene||||||
4380|Colville Sandstone|32750|4|Described|p306|||||||||
4380|Colville Sandstone|33586|4|Described|Table 1|||See also p15.||||||02-JUL-08
4380|Colville Sandstone|33587|6|Mentioned|p11|||||||||
4380|Colville Sandstone|33588|6|Mentioned|p11|||||||||
4380|Colville Sandstone|33589|4|Described|p12|||Middle Miocene||||||
4380|Colville Sandstone|33591|6|Mentioned|p10|||||||||
4380|Colville Sandstone|33592|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4380|Colville Sandstone|33595|4|Described|Table 1|||||||||
4380|Colville Sandstone|34742|6|Mentioned|Map legend|middle Miocene|middle Miocene|||||||
4380|Colville Sandstone|35097|6|Mentioned|Fig.4|||||||||
4380|Colville Sandstone|35496|4|Described|Table 1|||Also on p22.||||||02-JUL-08
4380|Colville Sandstone|35772|6|Mentioned|p11|||||||||
4380|Colville Sandstone|36200|6|Mentioned|p15|||||||||
4380|Colville Sandstone|36701|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
4380|Colville Sandstone|36890|3|Fully described|p416|||||||||
4380|Colville Sandstone|36902|6|Mentioned|p24|||||||||
4380|Colville Sandstone|38016|6|Mentioned|p92|||||||||
4380|Colville Sandstone|38482|6|Mentioned|p24|||||||||
4380|Colville Sandstone|38553|6|Mentioned|p43|||||||||
4380|Colville Sandstone|38602|6|Mentioned|p2|||||||||
4380|Colville Sandstone|39322|6|Mentioned|Fig.3|||||||||
4380|Colville Sandstone|42108|6|Mentioned|p322|||||||||
4380|Colville Sandstone|42265|6|Mentioned|p4|||? Replaced by Yarle Sandstone January 1990||||||
4380|Colville Sandstone|43065|5|Briefly described|p93|||||||||
4380|Colville Sandstone|44145|4|Described|p550 tab 4-27, p555,p556-7, p548|Early Miocene|Early Miocene|Northern margin Eucla Basin. Age from foraminifera fauna. Max known thickness 23m. Type section in creek 27 km west of Lake Colville.||||Grades laterally into Plumridge Formation (north) and Nullarbor Limestone (south).|Calcareous sandstone; lesser calcarenite, shale, siltstone and granule conglomerate.|08-OCT-15
4380|Colville Sandstone|44365|5|Briefly described|map legend||Early Miocene|||||||
4380|Colville Sandstone|44864|6|Mentioned|Map Legend||Miocene|||||||
4380|Colville Sandstone|45149|4|Described|p63|||See also Table 1, p16.||||||02-JUL-08
4380|Colville Sandstone|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Thin calcareous sandstone. Partly overlain and interfingers with Nullarbor Limestone. Age: 18.5-14.5Ma. Thickness: 25m. Geological Province: Eucla Basin.||||||03-MAR-10
4380|Colville Sandstone|62369|5|Briefly described|p410 Fig.4|Middle Miocene|Early Miocene|Geological Province: Eucla Basin||||||
4380|Colville Sandstone|64646|6|Mentioned|p23 Fig. 3, p24 Fig. 4|Miocene|Miocene|Geological Province: Eucla Basin.||||||08-FEB-10
4380|Colville Sandstone|65942|2|Defined|p77-78|||Equal to Nullarbor Limestone.||Of Eucla Group.||||
4380|Colville Sandstone|69598|6|Mentioned|p2, p9, p10, p11 Tb.1, p29 Tb.4|Middle Miocene|Early Miocene|Eucla Basin. Up to 25m thick. Potential carbon dioxide storage reservoir.||||Equivalent to the Plumridge Formation. Grades into and interfingers with the Nullarbor Limestone.|Calcareous sandstone, minor siltstone, claystones and calcarenites.|
4380|Colville Sandstone|69648|6|Mentioned|p25|||Of Lowry (1968, 1970). A conceptually [Yarle Sandstone] equivalent sediment in the northwestern part of the Eucla Basin, is believed to be pre-Tertiary in age (Benbow, 1990b).||||||
4380|Colville Sandstone|70397|5|Briefly described|p2-3,12|Middle Miocene|Middle Miocene|Eucla Basin. Depositional environment: intertidal and supratidal; cool-temperate, open-marine shelf.||Unit of Eucla Group.||Underlain by Wilson Bluff Limestone. Laterally grades outboard (S-ward) into Nullarbor Limestone.||
4380|Colville Sandstone|70771|5|Briefly described|p5|||||||Grades laterally into (equivalent to) the Rawlinna Member.|Calcareous sandstones.|
4380|Colville Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, calcarenite, sandstone|
4380|Colville Sandstone|71361|5|Briefly described|p5, p18|Middle Miocene|Early Miocene|Eucla Basin. This unit is lithologically similar to the Nullarbor Limestone but with higher siliciclastic content.||||Equivalent to (grades into) the Nullarbor Limestone.||
4428|Condren Sandstone|7433|5|Briefly described|p25 Fig.2, p32 Fig.8, p38, pp52-53.|Late Permian|Late Permian|Gregory Sub-basin, Canning Basin. Fluvial clastics. Outcrops are sparsely distributed and exhibit considerable facies change. May have potential as aquifer and for coal.||||Overlies Lightjack Formation. Is overlain by Hardman Formation.|Fluvial siltstones and fine silty sandstones; abundant Glossopteris fossils. Rare thin coal beds.|
4428|Condren Sandstone|22741|5|Briefly described|P28, Table3 P12||Late Permian|||||||
4428|Condren Sandstone|22764|4|Described|Table2,p9|Late Permian|Early Permian|250 m. Conformable on Lightjack Formation.||||||01-FEB-10
4428|Condren Sandstone|23766|5|Briefly described|p20|Permian|Permian|Parent: Liveringa Group.||||||17-NOV-08
4428|Condren Sandstone|29813|6|Mentioned|p7|||||||||
4428|Condren Sandstone|29817|4|Described|Table 2|||Permian||||||
4428|Condren Sandstone|29818|6|Mentioned|Map legend|Permian|Permian|||||||
4428|Condren Sandstone|29819|6|Mentioned|Map legend|Permian|Permian|||||||
4428|Condren Sandstone|30342|6|Mentioned|Table 20|||||||||
4428|Condren Sandstone|33518|4|Described|Table 1|||||||||
4428|Condren Sandstone|33519|6|Mentioned|Map legend|Permian|Permian|||||||
4428|Condren Sandstone|33962|6|Mentioned|p49|||Liveringa Fm.||||||
4428|Condren Sandstone|33965|4|Described|Table 1|||||||||
4428|Condren Sandstone|33966|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4428|Condren Sandstone|35120|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4428|Condren Sandstone|35124|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4428|Condren Sandstone|35205|6|Mentioned|Map legend|Permian|Permian|||||||
4428|Condren Sandstone|36225|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
4428|Condren Sandstone|38878|6|Mentioned|Map legend|Kazanian|Kazanian|||||||
4428|Condren Sandstone|40794|6|Mentioned|p91|||||||||
4428|Condren Sandstone|42183|6|Mentioned|p359|||||||||
4428|Condren Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
4428|Condren Sandstone|43173|6|Mentioned|54|Late Permian|Early Permian|||||||
4428|Condren Sandstone|43563|6|Mentioned|Fig.2,p5,Fig.9,p15||Late Permian|||||||
4428|Condren Sandstone|43932|4|Described|p9,Tb.1 p6||Permian|||||||
4428|Condren Sandstone|44143|4|Described|p.435 Table 4-19; p.446, Figure 4-102|Late Permian|Late Permian|Unit in Liveringa Group. Up to 130m thick; sandstone; low-energy fluvial or deltaic with some swampy conditions. Conformably overlies Lightjack Formation. Plant fossils including Gangamopteris and Glossopteris. Type section at Condren Pinnacles (LUCAS: 20deg 06' S, 127deg 39' E).||||||22-NOV-17
4428|Condren Sandstone|44998|14|Not recorded|p173|||||||||
4428|Condren Sandstone|45140|5|Briefly described|p67|Permian|Permian|Canning Basin. Fluvial deposits.||Liveringa Group.||Conformably overlies Lightjack Formation. Is overlain conformably by Godfrey Beds.||
4428|Condren Sandstone|45153|2|Defined|App.4-75|Late Permian|Late Permian|Previously mapped as Condren Sandstone Member (Casey & Wells, 1964).||||||
4428|Condren Sandstone|45158|3|Fully described|p18|||See also p36||||||17-MAR-20
4428|Condren Sandstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
4428|Condren Sandstone|48826|14|Not recorded|Figs,14,16,p.40|||||||||
4428|Condren Sandstone|49644|5|Briefly described|Table|||||||||
4428|Condren Sandstone|64643|5|Briefly described|p9|||Of Liveringa Group in SE Canning Basin only.||||||
4428|Condren Sandstone|64974|5|Briefly described|p148 Fig. 6|Tatarian|Ufimian|Of Liveringa Group. Geological Province: Canning Basin.||||||24-JUN-09
4428|Condren Sandstone|66949|4|Described|p4 Fig.2, p7, p24, p34, p46-47 Appx.2|Capitanian|Capitanian|See also p56 Appx.3, p60 Appx.4. SE Canning Basin. Formerly Condren Sandstone Member of Casey and Wells (1964). Type section detailed. Up to 130m thick; low energy fluvial or deltaic deposits, some swampy conditions. Late Permian: Gangamopteris and Glossopteris. Well-exposed in breakaways, cliffs, strike ridges, mesas, buttes, low hills. Biostratigraphic zonation. Available core detailed.||Unit in Liveringa Group.||Conformably overlies Lightjack Formation. Is overlain by Hardman Formation.|Sandstone, minor siltstone; coal seams; abundant plant macrofossils.|
4428|Condren Sandstone|70774|5|Briefly described|p9|Capitanian|Capitanian|SE Canning Basin only.||||Lightjack Formation underlies and lateral equivalent. Hardman Formation overlies.||
4428|Condren Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Liveringa Group.|||Fluvial to paralic or deltaic fossiliferous cross bedded and ripple marked fine to medium quartzose sandstone, with minor siltstone and conglomerate.|
4428|Condren Sandstone|71623|5|Briefly described|p343, 348, 349, p345 fig 3|Capitanian|Wordian|Canning Basin. Poorly fosiliferous, non-marine. Part of Cape Hay Clastic Cycle.||||Overlies Lightjack Formation unconformably.|Sandstone|
4428|Condren Sandstone|72505|5|Briefly described|p890|Wuchiapingian|Wuchiapingian|Canning Basin. Correlates to the Dulhuntyispora parvithola zone.||Liveringa Group||Overlies the Lightjack Formation, and partial lateral equivalent.. Overlain by the Hardman Formation.||17-MAR-20
4431|Cone Hill Granite|23722|4|Described|p12|Proterozoic|Proterozoic|Geological Province: Hooper Complex||||||
4431|Cone Hill Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
4431|Cone Hill Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4431|Cone Hill Granite|30897|5|Briefly described|p10|||Stratigraphic table||||||
4431|Cone Hill Granite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4431|Cone Hill Granite|36885|4|Described|p170|||||||||
4431|Cone Hill Granite|42814|5|Briefly described|p9|||||||||
4431|Cone Hill Granite|42815|5|Briefly described|map|||||||||
4431|Cone Hill Granite|43281|5|Briefly described|Map legend||Proterozoic|||||||
4431|Cone Hill Granite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex|||Coarse-grained porphyritic biotite granite.|
4431|Cone Hill Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
4431|Cone Hill Granite|71267|4|Described|GEOL_LUT_CSV files|||Geological province: Lamboo Province, Halls Creek Orogen. Restricted to the rocky peninsula in Cone Bay and a few nearby islands. Interpreted to be potentially related to porphyritic microgranite of the Wotjulum Porphyry. Weighted mean 207Pb/206Pb date of 1737+\-3 Ma, interpreted to be magmatic crystallisation age. See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv ansd geochron files.|1737+\-3 Ma (magmatic)||||Foliated coarsely porphyritic biotite muscovite monzogranite with small amphibolite xenoliths and small veins of tourmaline-bearing aplite and pegmatite|
4435|Congo Formation|23815|6|Mentioned|p281|||Geological Province: Byro Sub-basin. Mapped as the Wooramel Group.||||||18-APR-05
4435|Congo Formation|36890|6|Mentioned|p281|||||||||
4435|Congo Formation|37295|6|Mentioned|Table 2|||||||||
4435|Congo Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
4435|Congo Formation|45016|2|Defined|p.99-103||Artinskian|Tb. at back, Fig.65, p.69,74,75,77,90,97,106,115,121,148. (G50-6).||||||
4435|Congo Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
4460|Constantine Sandstone|23244|6|Mentioned|Fig.1,2,5|||of De Grey Group, Mallina Basin. Underlying unit Clearville Formation (u).||||||
4460|Constantine Sandstone|23348|4|Described|218|||||||||
4460|Constantine Sandstone|23598|4|Described|p8|||Of De Grey Group. Overlain by Mallina Formation. Geological Province: Pilbara Craton.||||||26-JUL-07
4460|Constantine Sandstone|23743|4|Described|p7|Archean|Archean|Of De Grey Group. Overlain by Mallina Formation. Geological Province: Mallina Basin. Max. thickness: 3500 m.||||||07-NOV-08
4460|Constantine Sandstone|23783|5|Briefly described|p3|||Of the De Grey Group.||||||
4460|Constantine Sandstone|23784|5|Briefly described|p31|Archean|Archean|Of De Grey Group.||||||07-NOV-08
4460|Constantine Sandstone|23789|4|Described|p18|Archean|Archean|Geological Province: Mallina Basin.||||||07-NOV-08
4460|Constantine Sandstone|23793|4|Described|p25|Archean|Archean|Age: c.2990Ma.  Of De Grey Group.  Max. thickness 3500m||||||07-NOV-08
4460|Constantine Sandstone|23794|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group. Geological Province Pilbara Craton.||||||07-NOV-08
4460|Constantine Sandstone|23936|5|Briefly described|p3, Fig.4|||Of the De Grey Group.Geological Province: Pilbara Craton.||||||26-JUL-07
4460|Constantine Sandstone|24025|4|Described|p8 Tb. 1|Archean|Archean|Of De Grey Group.  Max. thickness: 3500m. Poorly sorted coarse- to fine-grained subarkose and wacke. ferruginous clastic sedimentary rocks.  Geological Province: Pilbara Craton.||||||07-NOV-08
4460|Constantine Sandstone|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: De Grey Group. Geological Province: Pilbara Craton||||||07-NOV-08
4460|Constantine Sandstone|24140|5|Briefly described|p215|Archean|Archean|Originally included in the Whim Creek Group by Fitton et al (1975) when it contained the upper part of Cistern Formation.  Geological Province: Mallina Basin.||||||07-NOV-08
4460|Constantine Sandstone|24166|4|Described|p13|Archean|Archean|Of the De Grey Group. Geological Province: Mallina Basin.||||||11-JUN-14
4460|Constantine Sandstone|24184|4|Described|p715|Archean|Archean|Of the De Grey Group. Overlain by Mallina Formation. Geological Province: Mallina Basin. Age: ca.2990-2970Ma||||||07-NOV-08
4460|Constantine Sandstone|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Parent: De Grey Group. Age: ca. 2970-2945 Ma (Smithies et al, 2001). Geological Province: Mallina basin||||||07-NOV-08
4460|Constantine Sandstone|24190|5|Briefly described|p820 Fig.1|||Parent: De Grey Group||||||
4460|Constantine Sandstone|24327|5|Briefly described|Map Legend|Archean|Archean|Poorly sorted subarkose and wacke, lesser interbeds of shale, metamorphosed.  Parent: De Grey Group.  Age:<3020Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
4460|Constantine Sandstone|24349|5|Briefly described|Map legend|Archean|Archean|Of De Grey Group.   Age: <3020Ma.  Geological Province: Pilbara Craton||||||07-NOV-08
4460|Constantine Sandstone|24550|5|Briefly described|p36 Tb. 3.2|Archean|Archean|Included under the Group heading of Mallina (?). Conglomerate, sandstone. Age: ca 2975Ma. Geological Province: Mallina Basin, Pilbara Craton.||||||07-FEB-11
4460|Constantine Sandstone|30766|2|Defined|Appendix|Proterozoic|Proterozoic|||||||
4460|Constantine Sandstone|31310|6|Mentioned|p53|||||||||
4460|Constantine Sandstone|34829|6|Mentioned|p67|||||||||
4460|Constantine Sandstone|37373|4|Described|p80|||||||||
4460|Constantine Sandstone|39697|6|Mentioned|p19|||See also P101||||||
4460|Constantine Sandstone|41250|5|Briefly described|p29|||||||||
4460|Constantine Sandstone|42231|6|Mentioned|p334|||||||||
4460|Constantine Sandstone|43821|5|Briefly described|map legend|Archean|Archean|Of De Grey Group.||||||07-NOV-08
4460|Constantine Sandstone|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
4460|Constantine Sandstone|44863|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
4460|Constantine Sandstone|50370|5|Briefly described|Map Legend|Archean|Archean|Of De Grey Group (Pilbara Supergroup). Geological Province: Pilbara Craton||||||07-NOV-08
4460|Constantine Sandstone|60362|5|Briefly described|p1516, p1518 Fig.2|Archean|Archean|Mallina Basin.||||Is overlain conformably by Mallina Formation.|Medium- to coarse-grained wacke and conglomerate.|
4460|Constantine Sandstone|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Of the Croydon Group.  Age: >2.9Ga.   Geological Province: Pilbara Craton.||||||07-NOV-08
4460|Constantine Sandstone|61267|5|Briefly described|p71|||Lateral facies equivalent of Whim Creek Group. Intruded by Peawah Granodiorite. Geological Province: Pilbara Craton.||||||
4460|Constantine Sandstone|63372|4|Described|Map Legend|Archean|Archean|Of the De Grey Group. Geological Province: Whim Creek and Mallina Basin. Undivided fine to coarse grained clastic rocks; metamorphosed. Age: <2970Ma.||||||23-SEP-15
4460|Constantine Sandstone|63420|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (Pilbara Supergroup). Geological Province: Pilbara Craton. Wacke and subarkose, with local shale; metamorphosed; coarse-grained subarkosic sandstone, pebbly sandstone; sandstone and lesser siltstone.||||||07-NOV-08
4460|Constantine Sandstone|63441|4|Described|p5 Tb.1, p27|Archean|Archean|Basal unit of Croydon Group (Pilbara Supergp). Overlain by Mallina Formation (upper unit). Geol.prov: Mallina Basin, Pilbara Craton. Medium- to coarse-grained, poorly sorted subarkose to wacke, locally with thick conglomerate layers.||||||07-FEB-11
4460|Constantine Sandstone|63538|4|Described|p6 Fig. 3|Archaean|Archaean|Of Croydon Group. Underlain by Cattle Well Formation, overlain by Mallina Formation and Kialrah Rhyolite. Geological Province: Pilbara Craton. Sedimentary rocks.||||||19-APR-13
4460|Constantine Sandstone|64174|5|Briefly described|Map legend|Archean|Archean|Of the Croydon Group (De Grey Supergroup). Geological province: Mallina Basin. Sandstone and wacke, locally arkosic; local conglomerate; includes quartzite; metamorphosed. And wacke and sandstone, with local shale; metamorphosed.||||||07-NOV-08
4460|Constantine Sandstone|64580|4|Described|map legend||Mesoarchean|Laminated shale and siltstone, locally ferruginous and/or chlorite-rich; includes layers of iron formation, chlorite-quartz schist, chert and wacke; metamorphosed.||||||09-DEC-08
4460|Constantine Sandstone|65415|6|Mentioned|p119 Fig.1, p120 Fig.2.|Archean|Archean|||Unit in De Grey Group.||||
4460|Constantine Sandstone|66122|5|Briefly described|p75|Archean|Archean|Mount Goldsworthy area, NE Pilbara Craton.||Croydon Group.|||Dominantly conglomerate and sandstone, with minor mafic igneous and volcaniclastic rocks.|
4460|Constantine Sandstone|66217|5|Briefly described|p42.|||Mallina Basin.||Croydon Group.|||Coarse clastic rocks.|05-JUN-20
4460|Constantine Sandstone|67201|5|Briefly described|p7 Fig.4, p8, p12 Tb.1, p60|||In northwestern Pilbara Craton, De Grey Superbasin, West Pilbara Superterrane and East Pilbara Terrane. Old detrital zircons: 3795 Ma (Nelson 2000).||Of Croydon Group.|||Quartzites.|05-JUN-20
4460|Constantine Sandstone|68035|5|Briefly described|p291|Mesoarchean|Mesoarchean|Mallina Basin.||Of Croydon Group.||||
4460|Constantine Sandstone|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins. The 3 facies are mapped separately.||Of the Croydon Group.|||Wacke and subarkose, local shale; coarse-grained subarkosic sandstone, pebbly sandstone, and minor chert- and quartz-pebble conglomerate; sandstone and lesser siltstone, includes mafic detritus, turbidite and debris-flow deposits; all metamorphosed.|07-JAN-15
4460|Constantine Sandstone|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||Croydon Group|||Subarkosic quartz sandstone and wacke, with locally abundant shale; metamorphosed. Wacke and subarkose with local shale. Sandstone and siltstone interbedded with basaltic tuffaceous rocks including accretionary lapilli.|
4460|Constantine Sandstone|69185|4|Described|GEOL_LUT_CSV files||Mesoarchean|Geological Province: Pilbara Craton. Of Central Pilbara Tectonic Zone; Of Mallina Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2990-2940 Ma|Unit of Croydon Group.|||Coarse-grained wacke, quartz sandstone; locally quarzitic; conglomerate, laminated shale and siltstone, ferruginous siltstone, shale and iron formation; metamorphosed; basalt and local hyaloclastic breccia; metamorphosed.|
4460|Constantine Sandstone|69301|5|Briefly described|p5 Fig.3, p9 Tb.1|||Pilbara Craton. West Pilbara Superterrane. Mallina Basin.||Croydon Group|||Sedimentary rocks.|
4460|Constantine Sandstone|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of Mallina Basin, De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3015-2948 Ma (inferred)|Unit of Croydon Group.|||Sandstone and siltstone, interbedded with basaltic tuffaceous rocks; includes accretionary lapilli; metamorphosed|
4460|Constantine Sandstone|70022|6|Mentioned|p115-116|||Mallina Basin, West Pilbara Superterrane.|c.2.98 Ga.|Croydon Group.|||Quartz-rich metasandstone.|
4460|Constantine Sandstone|70775|4|Described|p12, p41, p44-p45, p48, p54-p57, p62|Mesoarchean|Mesoarchean|Previously interpreted to be equivalent to the Cistern Formation (Van Kranendonk., 2006). The authors however, argue against this correlation [see p45]. This unit overlies BIF and chert that has been correlated with the Cleaverville Formation.|3015-2955 Ma|||Overlain by the Mallina Formation.|Quartzite, wacke, arkosic sandstone and shale.|05-JUN-20
4460|Constantine Sandstone|71137|6|Mentioned|p5|Archean|Archean|Up to 1300m thick. See also references to Constantine Formation (p2, 5).||Croydon Group.||||
4460|Constantine Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||banded iron formation, arkose, conglomerate, greywacke|
4460|Constantine Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mallina Basin.|Max age 3015+/-5 Ma, 2948+/-5 Ma.|Croydon Group|||Sandstone and wacke, locally arkosic; local conglomerate; includes quartzite; metamorphosed.|
4460|Constantine Sandstone|72251|5|Briefly described|p54|Mesoarchean|Mesoarchean|Geological province: West Pilbara Superterrane, Pilbara Craton.||Unit of Croydon Group.||Overlain by Mallina Formation. Underlain unconformably by Cleaverville Formation. Correlable to Red Hill Volcanics and Warambie Basalt.||
4460|Constantine Sandstone|72668|6|Mentioned|p4, p22|||West Pilbara Superterrane, East Pilbara Terrane.||Croydon Group||Overlies the Cattle Well Formation. Overlain by the Kialrah Rhyolite and the Mallina Formation.||12-JAN-22
4465|Coobina Complex|41594|4|Described|p69|||||||||
4473|Coodardoo Formation|22897|6|Mentioned|102|||Geol province Bangemall Basin||||||
4473|Coodardoo Formation|22905|5|Briefly described|p52 Fig. 2, p53 Table 1|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Thick-bedded turbidite sandstone and minor siltstone.  Overlain by the Collier Subgroup. Conformably overlies the Ullawarra Formation.  Max. thickness: ~200m.  See also p54.||||||24-JAN-06
4473|Coodardoo Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
4473|Coodardoo Formation|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Jeeaila Sandstone Member. U'lying unit Curran Formation. Geological Province: Bangemall Basin. Max. thickness: 60 m.||||||
4473|Coodardoo Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 200m. Overlies the Ullawarra Formation. Unconformably overlain by the Backdoor Formation. Geological Province: Edmund Basin.||||||
4473|Coodardoo Formation|24183|2|Defined|p4 Fig.3, p6, p18|Calymmian|Statherian|Youngest population of detrital zircons dated at c.1713 Ma.  Age: 1620-1462 Ma. Max. Thickness: 370m. Overlies the Curran Member. Unconformably overlain by the Backdoor Formation.||||||21-MAR-11
4473|Coodardoo Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Ullawarra Formation. Overlain by Backdoor Formation.||||||
4473|Coodardoo Formation|29845|6|Mentioned|Table 68|||||||||
4473|Coodardoo Formation|29916|4|Described|p118|||||||||
4473|Coodardoo Formation|30881|4|Described|p526|||||||||
4473|Coodardoo Formation|32720|6|Mentioned|Table 1|||||||||
4473|Coodardoo Formation|32722|6|Mentioned|Fig.3|||Stromatolite||||||
4473|Coodardoo Formation|34124|4|Described|Table 1|||Upper Proterozoic||||||
4473|Coodardoo Formation|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4473|Coodardoo Formation|35982|6|Mentioned|Table 22|||||||||
4473|Coodardoo Formation|36551|6|Mentioned|p101|||||||||
4473|Coodardoo Formation|37460|4|Described|Table 3.VI|||||||||
4473|Coodardoo Formation|39210|5|Briefly described|Table 2|||||||||
4473|Coodardoo Formation|39370|5|Briefly described|p32|||||||||
4473|Coodardoo Formation|40089|2|Defined|p32|Mesoproterozoic|Mesoproterozoic|||||||
4473|Coodardoo Formation|40899|6|Mentioned|Fig.1|||||||||
4473|Coodardoo Formation|41360|6|Mentioned|p192|||||||||
4473|Coodardoo Formation|44142|4|Described|p312 Tb.4-4, p319-320|||Within Dooley Subgroup of Chuck (1984). Lenticular unit up to 370m thick, of near-shore proximal turbidites.||Top of Edmund Subgroup.||Overlies Curran Formation conformably. Is overlain by the Mucalana Subgroup.|Arenite, wacke; minor siltstone, shale, aphanitic mudstone.|13-MAR-18
4473|Coodardoo Formation|44319|14|Not recorded|map legend||Mesoproterozoic|Bangemall Group. M.Proterozoic.||||||
4473|Coodardoo Formation|50010|5|Briefly described|p55 Fig. 1|Mesoproterozoic|Mesoproterozoic|Sandstone.||||||
4473|Coodardoo Formation|50225|5|Briefly described|p387 Fig. 2, p394|||Uppermost unit of the Edmund Group (Bangemall Supergroup). Medium- to very thick-bedded turbidite sandstone and minor siltstone. Gradually overlies the Curran Member (Ullawarra Formation) below.  Max. thickness: 200m. See also p390.||||||07-FEB-11
4473|Coodardoo Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup).||||||07-NOV-08
4473|Coodardoo Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
4473|Coodardoo Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Overlies: Curran Member. Lithic quartz sandstone; minor siltstone and mudstone.||||||07-NOV-08
4473|Coodardoo Formation|63471|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group (Bangemall Supergroup). Includes the Curran Member which overlies the Ullawarra Formation. Geological Province: Edmund Basin. Thin- to very thick-bedded lithic quartz sandstone; minor siltstone and mudstone.||||||24-SEP-07
4473|Coodardoo Formation|63866|5|Briefly described|p162|||||Edmund Group||||
4473|Coodardoo Formation|63869|4|Described|p28, p38-39, p40, p42, Plate 1|Calymmian|Statherian|Originally Coodardoo Sandstone (Daniels, 1966); renamed as Coodardoo Formation by Muhling and Brakel (1985). Forms prominent ridges. 150-370 m thick. Type section is on the southern limb of the Wanna Syncline in Coodardo Gap. Minimum age from a dolerite sill (Wingate, 2002).|c.1620- >1070 Ma.|Topmost unit in Edmund Group.||Gradationally overlies Curran Member (Ullawarra Formation). Is unconformably overlain by Backdoor Formation (Collier Group).|Dominantly thick- to very thick-bedded, fine- to very coarse-grained lithic quartz sandstone and pebbly sandstone, interbedded with siltstone.|
4473|Coodardoo Formation|64580|4|Described|map legend||Mesoproterozoic|Of Edmund Group. Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert, and minor conglomerate.||||||09-DEC-08
4473|Coodardoo Formation|64728|5|Briefly described|p95 Fig.2, p105.|Mesoproterozoic|Mesoproterozoic|Deep-water siliciclastic and carbonate facies deposited below wave-base. Type section is at Coodardoo Gap, approximately 1.2 km northeast of Coodardoo Well.|Maximum depositional age between 1698-1677 Ma.|Unit in Edmund Group.||Overlies Ullawarra Formation. Is overlain by Backdoor Formation.|Thick-bedded, massive quartz sandstone, interbedded with thin beds of laminated siltstone.|
4473|Coodardoo Formation|65830|4|Described|p4, p7, p8, p10, p16-17; Plates 1,2|Calymmian|Statherian|Youngest unit of the Edmund Group. Thickness to 370m; thins to SE. Interpreted as turbidite fan deposits. A sill dated at 1070 Ma intrudes immediately below the Coodardoo Formation.|> 1070 Ma|Of the Edmund Group||Underlain gradationally by the Curran Member (Ullawarra Formation). Unconformably overlain by the Backdoor Formation (Collier Group).|Dominated by very thick to thick-bedded, very coarse to fine-grained lithic quartz sandstone and pebbly sandstone, interbedded with siltstone.|
4473|Coodardoo Formation|66241|6|Mentioned|pp1-4. |||||Unit in Edmund Group.||Overlies Ullawarra Formation. Is overlain by Backdoor Formation.||
4473|Coodardoo Formation|67136|5|Briefly described|Map legend.|||Edmund Basin.||Unit in Edmund Group.||Overlies Ullawarra Formation.|Thin- to very thick-bedded lithic quartz sandstone; minor siltstone and mudstone.|
4473|Coodardoo Formation|67374|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Thin- to very thick-bedded lithic quartz sandstone; minor siltstone and mudstone.|
4473|Coodardoo Formation|68285|5|Briefly described|Map Legend|Calymmian|Calymmian|Edmund Basin.||Of the Edmund Group.||Overlies Ullawarra Formation.|Thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone.|
4473|Coodardoo Formation|68286|5|Briefly described|Map Legend|Calymmian|Calymmian|Edmund Basin.||Of the Edmund Group||Overlies Ullawarra Formation|Thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone.|
4473|Coodardoo Formation|69003|5|Briefly described|p34|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Ullawarra Formation. Is overlain by Backdoor Formation (Collier Group).||
4473|Coodardoo Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Underlain by the Curran Member (Ullawarra Formation). Overlain by the Backdoor Formation (Collier Group).|Thin to very thick bedded lithic quartz sandstone; minor siltstone and mudstone.|05-MAY-14
4473|Coodardoo Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Devil Creek, Ullawarra and Discovery Formations as one unit.||Of the Edmund Group.|||Siltstone and mudstone; sandstone, dolostone, dolomitic mudstone, chert and minor conglomerate.|06-MAY-14
4473|Coodardoo Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Age derived from lithic quartz sandstone sample (148975.1.pdf)|1674 Ma +/- 24 Ma (SHRIMP)|Edmund Group||Overlies Curran Member, Disconformably overlain by Backdoor Formation|Siltstone and thin- to thick-bedded sandstone. Thin-very thickly bedded lithic quartz sandstone; local silicified sandstone and conglomerate.|
4473|Coodardoo Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 4.||Unit of Edmund Group.||||
4473|Coodardoo Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
4473|Coodardoo Formation|70019|6|Mentioned|p93|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen.||Unit of Edmund Group.||Uppermost unit of Edmund Group. Overlain by Collier Group. Underlain by Ullawarra Formation.||
4473|Coodardoo Formation|70795|4|Described|100k_geologyp_lut.csv|Mesoproterozoic|Mesoproterozoic|Also 100k_interpgeop_lut.csv, 148975.1.pdf, West Australian Craton, Edmund Basin|1456 Ma|Edmund Group||Overlies Ullawarra Formation, conformably overlies Curran Member, disconformably overlain by Backdoor Formation|Thin to very thick bedded lithic quartz sandstone, siltstone; minor mudstone.|
4473|Coodardoo Formation|70814|4|Described|p3, p5, p13-p15, p20, p22, p27, p33-p35|||Edmund Basin. Together with the Discovery, Devil Creek and Ullawarra Formations forms Depositional Package 4 of the Edmund Group. Outcrops around the core of the Wanna Syncline where it attains a maximum thickness of 370m. Deposited as deep-marine, shelf and submarine fan deposits with sandstones probably deposited in turbidity currents.||Edmund Group||Conformably overlies the Ullawarra Formation. Overlain by the Backdoor Formation. Unconformably overlain by the Collier Group.|Thin to very thickly-bedded, fine to very coarse-grained lithic quartz sandstone and pebbly sandstone interbedded with siltstone.|04-MAY-23
4473|Coodardoo Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, sandstone, dolostone|
4473|Coodardoo Formation|72705|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Overlies Ullawarra Formation. Is overlain by Backdoor Formation.||
4473|Coodardoo Formation|73442|6|Mentioned|p15|||Uppermost unit of Depositional Package 4.||Edmund Group||||
4481|Cooee Group|41066|6|Mentioned|2 of 2 J03|||||||||
4481|Cooee Group|41588|6|Mentioned|Table 1|||||||||
4554|Coolkilya Sandstone|14228|5|Briefly described|p8|Permian|Permian|||Kennedy Group||Overlies Baker Formation.||05-OCT-16
4554|Coolkilya Sandstone|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
4554|Coolkilya Sandstone|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Kennedy Group.||||||
4554|Coolkilya Sandstone|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Kennedy Group.||||||
4554|Coolkilya Sandstone|23726|4|Described|p38|Permian|Permian|Of Kennedy Group. Overlying unit Mungadan Sandstone. Underlying unit Baker Formation. Geological Province: Carnarvon Basin.||||||
4554|Coolkilya Sandstone|24044|6|Mentioned|p539|||Superseded by Coolkilya Sandstone.||||||
4554|Coolkilya Sandstone|34277|6|Mentioned|Table 1|||Permian||||||
4554|Coolkilya Sandstone|37294|6|Mentioned|p100|||||||||
4554|Coolkilya Sandstone|37295|6|Mentioned|p51|||Proposed usage.||||||
4554|Coolkilya Sandstone|37303|5|Briefly described|p65|||||||||
4554|Coolkilya Sandstone|39316|6|Mentioned|Fig.2|||||||||
4554|Coolkilya Sandstone|40617|6|Mentioned|Fig.1|||||||||
4554|Coolkilya Sandstone|41271|3|Fully described|p102|||Formerly "Coolkilya Greywacke"||||||
4554|Coolkilya Sandstone|41438|6|Mentioned|p105|||See also Fig.11||||||
4554|Coolkilya Sandstone|41632|4|Described|p1|||||||||
4554|Coolkilya Sandstone|42116|5|Briefly described|p28|||See also Fig.11||||||
4554|Coolkilya Sandstone|42392|6|Mentioned|p117|||See also Coolkilya Formation P116 - Part of Kennedy Group||||||
4554|Coolkilya Sandstone|42598|6|Mentioned|Fig 36(P 38)|||||||||
4554|Coolkilya Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
4554|Coolkilya Sandstone|43018|5|Briefly described|Table 1,p386|||||||||
4554|Coolkilya Sandstone|49644|5|Briefly described|Table|||||||||
4554|Coolkilya Sandstone|50620|5|Briefly described|p191|Late Permian|Early Permian|Of the Kennedy Group. Geological Province: Carnarvon Basin.||||||
4554|Coolkilya Sandstone|64974|5|Briefly described|p146, p147 Fig. 5|Ufimian|Ufimian|Of Kennedy Group. Geological Province: Carnarvon Basin.||||||24-JUN-09
4554|Coolkilya Sandstone|66189|5|Briefly described|p454, p455 Fig.2|Roadian|Kungurian|Lowest unit of the Kennedy Group. Overlies Byro Group; is overlain by Mungadan Sandstone. Shoreface-facies and fossiliferous.||||||27-AUG-15
4554|Coolkilya Sandstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes tan grey medium-grained sandstone.|
4554|Coolkilya Sandstone|67200|5|Briefly described|p7 fig 5, p47, p54, app 2 p5|Permian|Permian|Thermal conductivity of 2.86 W/mK||Kennedy Group||Overlies Baker Formation, overlain by Mungadan Sandstone|Bioturbated,parallel bedded, interbedded,  sandstone and siltstone.|
4554|Coolkilya Sandstone|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Kennedy Group.|||Comprises fine to very fine grained sandstone (commonly silty); minor siltstone and shale.|
4554|Coolkilya Sandstone|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Kennedy Group|||Fine to very fine grained sandstone (commonly silty); minor siltstone and shale.|
4554|Coolkilya Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, greywacke|
4554|Coolkilya Sandstone|72505|5|Briefly described|p890|Roadian|Roadian|Southern Carnarvon Basin. Correlates with the Microbaculispora villosa zone.||Kennedy Group||Overlies the Byro Group. Overlain by the Mungadan Sandstone.||
4554|Coolkilya Sandstone|72910|4|Described|p3-4, p6, p10-11, p17-20, p25, 27.|Roadian|Kungurian|Shown as being part of the Merlinleigh Sub-basin. Thickness 110-285m. Type section located at East side, Wandagee Hill, 23d50m10sS, 114d25m50sE.  Age derived from type section brachiopod fauna (Archbold 1995a) and shown as Kungurian to Ufimian. See also p30, p33, p38, p41.||Kennedy Group||Overlies Wandagee Formation. Conformably overlies Baker Formation and underlies Mungadan Sandstone.|Greenish-grey, fine to very fine silty sandstone, minor siltstone and shale.|
4558|Cooloongup Sand|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Geological Province: Perth Basin.||||||24-NOV-09
4558|Cooloongup Sand|32575|2|Defined|p9|Quaternary|Quaternary|See also p55.||||||06-AUG-07
4558|Cooloongup Sand|36293|4|Described|p216|||||||||
4558|Cooloongup Sand|40400|6|Mentioned|p109|||Of Passmore (1970). Overlain by Bridport Calcilutite - bioturbated to gradational contact. Geological Province: Perth Basin.||||||06-AUG-07
4558|Cooloongup Sand|40401|6|Mentioned|p122|||||||||
4558|Cooloongup Sand|40731|5|Briefly described|p34|||||||||
4558|Cooloongup Sand|41200|5|Briefly described|p27|||Overlain by Bridport Calcilutite - bioturbated to gradational, conformable contact.||||||06-AUG-07
4558|Cooloongup Sand|41502|5|Briefly described|p96|||||||||
4558|Cooloongup Sand|42009|5|Briefly described|p75|||||||||
4558|Cooloongup Sand|44144|4|Described|p501 Tb.4-21|Holocene|Pleistocene|Type Section: Rockingham Bore RT20 32o16'48''S 115o46'53''E. 6.5-10.4 m of shallow marine deposits.||Kwinana Group||Overlies Tamala Limestone.  Overlain by Safety Bay Sand.|Grey to brown, fine- to coarse-grained feldspathic sand.|
4558|Cooloongup Sand|61521|6|Mentioned|p41|||Mentioned as possibly being a remnant deposit (muddy quartz sand) that infills a depression within the limestone that forms the Garden Island Ridge.||||||
4558|Cooloongup Sand|69788|3|Fully described|p1023, p1025, p1027, p1029 Fig.4|Pleistocene|Pleistocene|See also p1032-1035, p1037. Of Passmore (1970). Type locality in the Rockingham area. Later called Eaton Sand (Semeniuk, 1983) but the name lacked precedence and lapsed. 0.5-2m thick. Sediment was either derived from dissolution of Tamala Limestone eolianites, or (less likely) wind-blown from inland areas. OSL ages by Lipar and Webb (2014); also a C-14 age of >35ka (Semeniuk, 1983).|>49.5 +/- 10.5 ka and 31 +/- 6.5 ka.|||Overlies Tamala Limestone. Is overlain locally by Burragenup Member.|Decimetres- to metres-thick beds of yellow-red-brown loose quartz sand: quartz grains with very thin ferruginous coating.|
4558|Cooloongup Sand|69840|4|Described|p183, p185, p187-188, p187 Tb.1|Pleistocene|Pleistocene|See also p196 Fig.13, p197, p190, p198, p200. Considered to be sand released from dissolution of Tamala Limestone members, during pinnacle formation. Dating using OSL geochronology. Other dated sample gave age of /= 0.049+/- 0.010.5 Ma. Marine Isotope stage 2-4. On p186 Fig.3 diagram shown as not part of any dune system.|0.03100 +/- 0.00650 Ma|||Overlies Tamala Limestone and underlies Burragenup Member, Safety Bay Sand.|Loose orange-red-brown quartz sand.|
4565|Coolyena Group|12758|5|Briefly described|p22, p3 Fig. 3|Early Cretaceous|Early Cretaceous|Transgressive over the Warnbro Group. Comprises Osborne Formation, Molecap Greensand, Gingin Chalk and Poison Hill Greensand; also includes Lancelin Formation further west. See also p10 Fig. 10.||||||22-JUL-09
4565|Coolyena Group|12759|4|Described|pp38-42|Cretaceous|Cretaceous|Defined by Cockbain and Playford (1973). Shallow marine deposition.|||Comprises Osborne and Lancelin Formations; Molecap and Poison Hill Greensands, and Gingin Chalk.|Unconformably overlies Warnbro Group.||12-MAY-14
4565|Coolyena Group|14227|5|Briefly described|Enclos. 2|Late Cretaceous|Early Cretaceous|Includes Breton Marl, Poison Hill Greensand, Lancelin Formation, Gingin Chalk, Molecap Greensand, Osborne Formation||||||07-FEB-11
4565|Coolyena Group|22814|5|Briefly described|fig2|Cretaceous|Cretaceous|||||||
4565|Coolyena Group|23279|4|Described|p30-1|Maastrichtian|Albian|(Cockbain and Playford, 1973).||||||
4565|Coolyena Group|23816|5|Briefly described|p249|Late Cretaceous|Late Cretaceous|Geological Province: Perth Basin. Underlying unit: Warnbro Group.||||||27-APR-05
4565|Coolyena Group|24160|5|Briefly described|p94|Cretaceous|Cretaceous|Perth Basin.|||Includes Osborne Formation.||Glauconitic sandstone, argillaceous rocks, chalk.|
4565|Coolyena Group|24443|5|Briefly described|Fig.30|Late Cretaceous|Early Cretaceous|Unconformably overlies Warnbro Group. Overlain by Cainozoic undifferentiated shelf carbonates. Geological Province: Perth Basin.||||||
4565|Coolyena Group|29382|6|Mentioned|Table 10|||||||||
4565|Coolyena Group|29693|6|Mentioned|Fig.7|||||||||
4565|Coolyena Group|30188|2|Defined|p75|Cretaceous|Cretaceous|Includes Osborne Fm, Gingin Chalk, Molecap & Poison Hill Greensands.||||||22-SEP-09
4565|Coolyena Group|30268|6|Mentioned|p44|||||||||
4565|Coolyena Group|31153|6|Mentioned|Fig. 57|||Table refers Cockbain & Playford (1973)||||||
4565|Coolyena Group|31238|4|Described|p27|||||||||
4565|Coolyena Group|35653|6|Mentioned|p1094|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
4565|Coolyena Group|35968|6|Mentioned|Table 4|||||||||
4565|Coolyena Group|35970|6|Mentioned|p77|||See also Table 12.||||||
4565|Coolyena Group|35973|6|Mentioned|p93|||||||||
4565|Coolyena Group|36100|6|Mentioned|Fig.2|||||||||
4565|Coolyena Group|36265|5|Briefly described|Fig.3.26|Late Cretaceous|Late Cretaceous|Includes Osborne Formation, Molecap Greensand, Gingin Chalk and Poison Hill Greensand. Geological province: Perth Basin.||||||04-MAR-08
4565|Coolyena Group|36293|2|Defined|p177|Late Cretaceous|Late Cretaceous|||||||
4565|Coolyena Group|36890|3|Fully described|p249|||||||||
4565|Coolyena Group|37104|6|Mentioned|Fig.3|||||||||
4565|Coolyena Group|40348|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
4565|Coolyena Group|40349|4|Described|p16|||||||||
4565|Coolyena Group|40877|5|Briefly described|p55|||||||||
4565|Coolyena Group|40992|6|Mentioned|Fig.5|||||||||
4565|Coolyena Group|41195|6|Mentioned|Fig.2|||||||||
4565|Coolyena Group|41728|6|Mentioned|p442|||See also Fig.3||||||
4565|Coolyena Group|41989|4|Described|p113|||||||||
4565|Coolyena Group|42075|5|Briefly described|Fig.7 P247|||||||||
4565|Coolyena Group|42123|6|Mentioned|p19|||||||||
4565|Coolyena Group|42687|6|Mentioned|map legend|||||||||
4565|Coolyena Group|42688|6|Mentioned|map legend|Cretaceous||||||||
4565|Coolyena Group|42995|6|Mentioned|p19|||||||||
4565|Coolyena Group|43031|5|Briefly described|Fig.2.|||||||||
4565|Coolyena Group|43062|5|Briefly described|Table 2,p18|||||||||
4565|Coolyena Group|43347|4|Described|9|Late Cretaceous|Early Cretaceous|||||||
4565|Coolyena Group|43700|6|Mentioned|p25|||||||||
4565|Coolyena Group|44144|5|Briefly described|p503 Tb.4-21, p509 fig 4-145, p516-517 |Cretaceous|Cretaceous||||Includes Osborne and Lancelin Formations; Molecap and Poison Hill Greensands; Gingin Chalk.||Glauconitic sandstone and argillaceous rocks and chalk.|
4565|Coolyena Group|50108|5|Briefly described|Map legend|Late Cretaceous|Late Cretaceous|Geological Province: Perth Basin.||||||
4565|Coolyena Group|60376|5|Briefly described|p17 Fig. 4.|Cretaceous|Cretaceous|Geological Province: Perth Basin. Overlain unconformably by Late Cretaceous carbonates. Underlain unconformably by Leederville Formation (Warnbro Group).||||||07-FEB-11
4565|Coolyena Group|61155|5|Briefly described|p15|||Age is Pre-Cainozoic. Geological Province: Perth Basin.||||||03-MAR-10
4565|Coolyena Group|61811|5|Briefly described|p3 Fig.2, pp54-57.|Campanian|Aptian|Northern Perth Basin. Mis-spelt as Cooleyna Group in Fig.2.|||Includes Osborne Formation, Molecap Greensand, Lancelin Formation, Gingin Chalk and Poison Hill Greensand.|Unconformably overlies Warnbro Group.||
4565|Coolyena Group|64580|4|Described|map legend||Late Cretaceous|Undivided; chalk, greensand, glauconitic sandstone, siltstone, marl; characteristically glauconitic; includes OSBORNE and LANCELIN FORMATIONS, MOLECAP and POISON HILL GREENSANDS, and GINGIN CHALK.||||||09-DEC-08
4565|Coolyena Group|67135|5|Briefly described|p5 Fig.7, p33 Fig.42.|Cretaceous|Cretaceous|Perth Basin. A confining bed for aquifers in the Perth Basin.||||Overlies Leederville Formation.||
4565|Coolyena Group|67340|6|Mentioned|p6|Late Cretaceous|Early Cretaceous|Northern Perth Basin. Appears as Cooleyna Group on p6.|||Osborne, Lancelin Formations, Molecap, Poison Hill Greensands, Gingin Chalk.|||
4565|Coolyena Group|67925|5|Briefly described|Ch2 p10 fig 4, Ch4 p8 fig 2|Cenomanian|Aptian|||||Unconformably overlies the Warnbro Group and the Leederville Formation. Unconformably overlain by the Kings Park Formation.||
4565|Coolyena Group|69081|5|Briefly described|p737 Fig.1|Late Cretaceous|Early Cretaceous|Geol. Prov: Perth Basin|||Osborne Formation|unconformably overlies Warnbro Group||
4565|Coolyena Group|69182|5|Briefly described|Ch2 p3, Ch2 p9|Late Cretaceous|Lower Cretaceous|Perth Basin. See also Ch2 p15, Ch2 p45, Ch2 p55, Ch2 p57.|||Includes the Dandaragan Sandstone, the Osborne Formation, the Molecap Greensand, Gingin Chalk, Poison Hill Greensand and the Lancelin Formation.|Unconformably overlies the Warnbro Group. Unconformably overlain by the Kings Park Shale.|Sandstones, greensands and chalk.|
4565|Coolyena Group|69297|6|Mentioned|p174, p175, p189|Cenomanian|Hauterivian|Vlaming Sub-basin. Deposited in a deep marine or deltaic environment. |||Includes the Osborne Formation, Molecap Greensand, Gingin Chalk and the Poison Hill Greensand.|Overlies the Warnbro Group.||
4565|Coolyena Group|70097|5|Briefly described|p19 Fig.3, p20 Fig.4|Maastrichtian|Aptian|Perth Basin. Dandaragan Trough, Beermullah Trough, Mandurah Terrace and Vlaming Sub-basin.|||Dandaragan Sandstone, Osborne Formation, Molecap Greensand, Gingin Chalk, Poison Hill Greensand, Lancelin Formation|Overlies Warnbro Group. Is overlain by Kings Park Shale.|Includes sandstone and limestone.|12-SEP-17
4565|Coolyena Group|70099|5|Briefly described|Fig.4|Maastrichtian|Aptian|Mentelle 7b, 8 and 9 Supersequences.|||Osborne Formation; Molecap and Poison Hill Greensands; Gingin Chalk.|Overlies Warnbro Group.||
4565|Coolyena Group|70128|5|Briefly described|p449, p456, p458-462|Late Cretaceous|Early Cretaceous|Central Perth Basin. Modelled thickness distribution histogram.||||Unconformably overlies Leederville Formation (Warnbro Group). Is overlain unconformably by Kings Park Formation.||
4565|Coolyena Group|71377|5|Briefly described|p7, p9|Late Cretaceous|Early Cretaceous|Mandurah Terrace, Perth Basin.|||Includes the Osborne Formation.|||
4565|Coolyena Group|71958|5|Briefly described|p34-p35, p41|Maastrichtian|Aptian|Vlaming Sub-basin.||||Overlies the Warnbro Group.||
4565|Coolyena Group|72034|5|Briefly described|500k_interpgeop16_lut|Maastrichtian|Albian|Perth Basin.  Age from biostratigraphy.|||Includes Lancelin Formation, Osborne Formation.||Chalk, greensand, glauconitic sandstone, siltstone, marl; characteristically glauconitic.|
4586|Coomarie Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
4586|Coomarie Sandstone|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
4586|Coomarie Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
4586|Coomarie Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
4586|Coomarie Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Birrindudu Group. Overlies Talbot Well Formation; unconformably overlain by Stirling Sandstone. Geological Province: Birrindudu Basin.||||||22-DEC-08
4586|Coomarie Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
4586|Coomarie Sandstone|29804|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
4586|Coomarie Sandstone|29805|4|Described|Table 1|||||||||
4586|Coomarie Sandstone|29809|6|Mentioned|Table 1|||||||||
4586|Coomarie Sandstone|29811|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
4586|Coomarie Sandstone|29813|4|Described|Table 2|||||||||
4586|Coomarie Sandstone|29818|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4586|Coomarie Sandstone|31361|4|Described|Table 1|||||||||
4586|Coomarie Sandstone|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4586|Coomarie Sandstone|36551|6|Mentioned|Table 12|||||||||
4586|Coomarie Sandstone|45140|2|Defined|p13, p39-40, p42-43, p54, Appx.p18-19|||Blake et al. (1975). Named after Coomarie Range and Coomarie Spring. Birrindudu Basin. The type section is at latitude 19deg 15'S, across the W limb of the syncline between longitudes 129deg 12'10"E and 129deg 13'10"E, Tanami sheet area. 2500m thick.||Birrindudu Group.||Conformably overlies Talbot Well Formation. Is overlain unconformably by Antrim Plateau Volcanics. Tentatively correlated with Pindar Beds.|Sublithic arenite and minor quartz arenite, mainly medium-grained, thin-bedded to flaggy, showing cross-bedding and ripple marks; siltstone and shale. Shale pellets common in the sublithic arenite.|
4586|Coomarie Sandstone|46788|6|Mentioned|p11|||||||||
4586|Coomarie Sandstone|46864|4|Described|p38|||||||||
4586|Coomarie Sandstone|48950|2|Defined|p38|Neoproterozoic|Neoproterozoic|||||||
4586|Coomarie Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Basalt or sandstone; sandstone - sublithic arenite, minor quartz arenite, siltstone and shale; medium-grained, ripple marks and mud cracks.||||||07-NOV-08
4586|Coomarie Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group.||||||07-NOV-08
4586|Coomarie Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Basalt sandstone; sandstone||||||07-NOV-08
4586|Coomarie Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Basalt; sandstone: sublithic arenite, minor quartz arenite, siltstone and shale.||||||07-NOV-08
4586|Coomarie Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group. Geological Province: Birrindudu Basin.||||||
4586|Coomarie Sandstone|61861|4|Described|p5, p22, p24, p3 Table 1|Statherian|Statherian|Forms prominent ridges. 400 m thick. The basalt horizon is shown by magnetic data to be folded with the rest of the stratigraphy, thus being part of the Formation and not part of Antrim Plateau Volcanics as shown in the first edition of the map.||Topmost unit in Birrindudu Group.|||Sublithic arenite and minor quartz arenite; locally includes a thin basalt horizon.|03-APR-12
4586|Coomarie Sandstone|63261|5|Briefly described|p5 Fig. 2, p9 Fig. 5, p17|||Of Birrindudu Group. Thickness: 400m. Geological province: Victoria-Birrindudu Basin.||||||07-FEB-11
4586|Coomarie Sandstone|64662|5|Briefly described|p30 Fig. 3|Statherian|Statherian|Of the Birrindudu Group. Geological Province: Tanami region.||||||07-FEB-11
4586|Coomarie Sandstone|64675|6|Mentioned|Fig.2|||||||||
4586|Coomarie Sandstone|65074|4|Described|p349, p351 fig 4-37, p352, p354 Tb. 4-11|Mesoproterozoic|Mesoproterozoic|Of North/Centre Birrindudu Basin.  2500m thick. Type section: syncline south of Browns Range (N.T.).||Birrindudu Group||Overlies Talbot Well Formation (conformably). Overlain by Antrim Plateau Volcanics (unconformably).|Sublithic arenite; minor quartz arenite, siltstone, shale.|
4586|Coomarie Sandstone|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; weakly magnetic sandstone, and basalt or magnetite-rich sandstone that is moderately magnetic; overlies the Talbot Well Formation||||||02-FEB-10
4586|Coomarie Sandstone|65324|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
4586|Coomarie Sandstone|65326|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
4586|Coomarie Sandstone|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
4586|Coomarie Sandstone|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
4586|Coomarie Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Birrindudu Group.||Overlies Talbot Well Formation. Is unconformably overlain by Stirling Sandstone of Limbunya Group.||
4586|Coomarie Sandstone|65349|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
4586|Coomarie Sandstone|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
4586|Coomarie Sandstone|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
4586|Coomarie Sandstone|65352|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; overlies the Talbot Well Formation||||||12-APR-10
4586|Coomarie Sandstone|65353|5|Briefly described|Map legend|Statherian|Statherian|2 unnamed units, only one shown on map; weakly magnetic sandstone; overlies the Talbot Well Formation||||||
4586|Coomarie Sandstone|65354|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
4586|Coomarie Sandstone|65355|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; weakly magnetic sandstone (shown on map), and basalt or magnetite-rich sandstone (not shown on map) that is moderately magnetic; overlies the Talbot Well Formation||||||02-FEB-10
4586|Coomarie Sandstone|65356|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group; overlies the Talbot Well Formation||||||12-APR-10
4586|Coomarie Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Birrindudu Group.||Overlies Talbot Well Formation. Is unconformably overlain by Antrim Plateau Volcanics.|Sandstone; basalt or magnetite rich sandstone.|
4586|Coomarie Sandstone|68733|6|Mentioned|p187 Fig.6|||||Of the Birrindudu Group.||||
4586|Coomarie Sandstone|69426|6|Mentioned|p11:5 Fig.11.4, |||In Blake et al. (1979).||Birrindudu Group.||||12-JUL-16
4586|Coomarie Sandstone|69432|5|Briefly described|p17:2, 4-5|Paleoproterozoic|Paleoproterozoic|Exposed N of the Coomarie Range and between the Pargee and Browns Ranges, Birrindudu Basin. Forms prominent ridges. Up to c.2500m thick.||Birrindudu Group.|||Sublithic sandstone; minor medium-grained and cross-bedded quartz sandstone; minor siltstone and shale.|12-JUL-16
4586|Coomarie Sandstone|69673|6|Mentioned|p48 fig 35|||||Birrindudu Group||Unconformably overlain by Stirling Sandstone, overlies Talbot Well Formation||
4586|Coomarie Sandstone|70291|4|Described|p180|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Magnetic data indicates presence of a 200m thick sill; age unknown.||Unit of Birridudu Group.|||Sublithic sandstone and quartz arenite|
4586|Coomarie Sandstone|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.|||Sublithic quartz sandstone, quartz sandstone.|
4586|Coomarie Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Birrindudu Group.|||Shallow marine cross bedded and rippled medium to fine grained sublithic sandstone with pellets of red and green siltstone, minor siltstone and shale|
4586|Coomarie Sandstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Birrindudu Group.||||
4586|Coomarie Sandstone|71349|5|Briefly described|p725|||||Birrindudu Group.||||
4590|Coomberarie Formation|23569|4|Described|p4 Tb. 1|Proterozoic|Proterozoic|Parent: Badgeradda Group.   Silty sandstone||||||
4590|Coomberarie Formation|24114|5|Briefly described|p8|Neoproterozoic|Mesoproterozoic|Of Badgeradda Group. Geological Province: Yilgarn Craton.||||||
4590|Coomberarie Formation|29690|4|Described|p13|||||||||
4590|Coomberarie Formation|30949|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4590|Coomberarie Formation|36293|6|Mentioned|p77|||||||||
4590|Coomberarie Formation|36872|4|Described|p71|||||||||
4590|Coomberarie Formation|37460|5|Briefly described|p177|||||||||
4590|Coomberarie Formation|38494|4|Described|p26|||||||||
4590|Coomberarie Formation|38998|6|Mentioned|p14|||||||||
4590|Coomberarie Formation|40336|5|Briefly described|p15|||||||||
4590|Coomberarie Formation|40340|6|Mentioned|p8|||||||||
4590|Coomberarie Formation|40343|6|Mentioned|p10|||||||||
4590|Coomberarie Formation|43835|5|Briefly described|Map Legend||Proterozoic|||||||
4590|Coomberarie Formation|44142|5|Briefly described|p328 Tb.4-5|||||Badgeradda Group|||Silty sandstone.|
4590|Coomberarie Formation|45015|2|Defined|map, p.19-22, map legend||Proterozoic|Of Badgeradda Group. Siltstone and fine-grained  greywacke. Conformably overlies Woodrarrung Sandstone; conformably underlies Yarrawolya Formation. Max. thickness: 4985ft in type section. Geol. Prov: Carnarvon Basin.||||||31-MAY-06
4590|Coomberarie Formation|48823|3|Fully described|p3 Tb. 1, p13, map legend|Mesoproterozoic|Mesoproterozoic|Of Badgeradda Group. Grey to brown and reddish-white, thin bedded and fine-grained sandstone, with x-stratification in places. Conformably overlies Woddrarrung Formation; underlies Yarrawolya Formation. Thickness: ~6900ft. See also p10 Tb. 2.||||||28-NOV-06
4590|Coomberarie Formation|61958|5|Briefly described|Map sheet 1|Neoproterozoic|Neoproterozoic|Of the Badgeradda Group.||||||21-MAR-06
4590|Coomberarie Formation|64580|4|Described|map legend||Mesoproterozoic|Of Badgeradda Group. Silty sandstone, siltstone.||||||09-DEC-08
4590|Coomberarie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
4590|Coomberarie Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Badgeradda Basin.||Badgeradda Group|||Silty sandstone, siltstone.|
4593|Coomberdale Subgroup|24160|5|Briefly described|p21, 25, 28|Proterozoic|Proterozoic|Formerly Dudawa Beds. 1500 m thick. Contains stromatolites at many localities, but precise age is unknown.||Moora Group|Mokadine Formation, Winemaya Quartzite, Campbell Sandstone, Noingara Siltstone, Noondine Chert, Jingemia Dolomite, Coomberdale Chert|Unconformably overlies Billeranga Subgroup.||
4593|Coomberdale Subgroup|24410|5|Briefly described|p139, p142 Tb. 60|Proterozoic|Proterozoic|Of the Moora Group. Includes: Mokadine Formation, Winemaya Quartzite, Campbell Sandstone, Noingara Siltstone, Noondine Chert and Jingemia Dolomite.  Parts formerly mapped as Coomberdale Chert and Dudawa Beds.||||||24-NOV-09
4593|Coomberdale Subgroup|24526|5|Briefly described|p112 Fig. 9|Neoproterozoic|Neoproterozoic|Of the Moora Group.  Overlies the Billeringa Subgroup. Age: >800Ma.||||||
4593|Coomberdale Subgroup|40307|6|Mentioned|p62|||||||||
4593|Coomberdale Subgroup|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
4593|Coomberdale Subgroup|40347|2|Defined|p19|Mesoproterozoic|Mesoproterozoic|||||||
4593|Coomberdale Subgroup|40349|4|Described|p13|||||||||
4593|Coomberdale Subgroup|42687|6|Mentioned|map legend|||||||||
4593|Coomberdale Subgroup|42688|6|Mentioned|map legend|||||||||
4593|Coomberdale Subgroup|44138|4|Described|p272|||Mature upward-fining siliciclastic-dolomitic, paralic sequence. 1500m thick.||Moora Group (upper)||Overlies Billeranga Subgroup (disconformably).|Sandstone, siltstone, dolomite, and silicified dolomite. Stromatolites occur.|
4593|Coomberdale Subgroup|64580|4|Described|map legend||Mesoproterozoic|Of Moora Group. Sandstone, siltstone, dolostone, stromatolitic dolostone and silicified dolostone.||||||09-DEC-08
4593|Coomberdale Subgroup|70796|5|Briefly described|500k_interpgeop14_lut.csv|Neoproterozoic|Neoproterozoic|Moora Basin, Pinjarra Orogen. Affected by the Leeuwin Orogeny.|ca. 1000  531 Ma (inferred)|Moora Group|||Sandstone, siltstone, dolostone, stromatolitic dolostone and silicified dolostone.|
4593|Coomberdale Subgroup|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, crystalline dolostone/dolomite, chert, sandstone|
4593|Coomberdale Subgroup|71269|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pinjarra Orogen. Of Moora Basin. Events: Leeuwin Orogeny (780-515 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|1600-541 Ma (inferred)|Unit of Moora Group.|||Sandstone, siltstone, dolostone, stromatolitic dolostone and silicified dolostone|
4593|Coomberdale Subgroup|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Mesoproterozoic|Moora Basin.||Moora Group|||Sandstone, siltstone, dolostone, stromatolitic dolostone and silicified dolostone.|
4597|Coonabildie Formation|23156|5|Briefly described|p9-10|Mesoproterozoic|Mesoproterozoic|Restricted to the south eastern corner of BULLEN.||||||
4597|Coonabildie Formation|24017|6|Mentioned|p11|||||||||
4597|Coonabildie Formation|24535|5|Briefly described|p2, 4|||Of Salvation Group. Previously included in Kahrban Subgroup and previously correlated with Sunbeam Group (Hocking and Jones, 2002).||||||26-NOV-13
4597|Coonabildie Formation|35596|4|Described|p8|||||||||
4597|Coonabildie Formation|37022|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4597|Coonabildie Formation|37026|6|Mentioned|p5|||||||||
4597|Coonabildie Formation|37460|6|Mentioned|p172|||||||||
4597|Coonabildie Formation|38515|4|Described|p15|||||||||
4597|Coonabildie Formation|38516|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4597|Coonabildie Formation|40089|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|||||||
4597|Coonabildie Formation|40354|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
4597|Coonabildie Formation|40355|4|Described|p11|||||||||
4597|Coonabildie Formation|43209|5|Briefly described|map legend||Mesoproterozoic|Of Kahrban Subgroup.||||||28-JUL-08
4597|Coonabildie Formation|43229|5|Briefly described|Map Legend||Mesoproterozoic|Of Kahrban Subgroup.||||||17-JUL-08
4597|Coonabildie Formation|43492|4|Described|9,10||Proterozoic|||||||
4597|Coonabildie Formation|44142|5|Briefly described|p315 Tb.4-4, p324|||110m thick near-shore pro-grading delta, submarine fan deposits. Poorly exposed. ||Kahrban Subgroup||Overlies Earaheedy Group and Scorpion Subgroup unconformably. Correlated with Collier Subgroup. Is overlain conformably by Marlooyanoo Formation.|Siltstone, medium grained sandstone; minor shale, chert, carbonate.|
4597|Coonabildie Formation|50188|4|Described|p15, p16|||Formerly of Kahrban Subgroup tog. with Marlooyanoo Fm. However the two formations were indistinguishable from each other, hence Marlooyanoo Fm has been abandoned. Now of Sunbeam Gp. Underlies Brassey Range Fm. Max.thickness: 250m+. Geol.Prov:Officer Basin||||||17-JUL-08
4597|Coonabildie Formation|50195|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group (Bangemall Supergroup).  Siltstone and fine-grained lithic sandstone. Geological Province: Salvation Basin.||||||28-JUL-08
4597|Coonabildie Formation|50319|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group. Siltstone and fine-grained lithic sandstone, commonly rippled; coastal and fluvial deposits.||||||
4597|Coonabildie Formation|50334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. Geological Province: Officer Basin, Centralian Superbasin.||||||
4597|Coonabildie Formation|62453|6|Mentioned|p52|||Of the Salvation Group.||||||
4597|Coonabildie Formation|63866|4|Described|p163|Ectasian|Calymmian|Bangemall Basin. SHRIMP age is interpreted as the maximum depositional age for this formation.|1330 +/- 70 Ma (SHRIMP U-Pb, Nelson, 2002)|Salvation Group||Overlain by the Brassey Range Formation.|Sandstones.|
4597|Coonabildie Formation|64283|5|Briefly described|p53|||Previously the "Kahrban Subgroup" of Williams (1990). Forms basal unit of Sunbeam Group. Conformably overlain by Brassey range Formation.||||||07-FEB-11
4597|Coonabildie Formation|64580|4|Described|map legend||Mesoproterozoic|Of Salvation Group. Sandstone, micaceous siltstone, and shale.||||||17-NOV-08
4597|Coonabildie Formation|64655|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Salvation Group. Siltstone and fine-grained lithic sandstone, commonly rippled; coastal to fluvial deposits.||||||
4597|Coonabildie Formation|64772|5|Briefly described|p13, Plate 1  legend|Mesoproterozoic|Mesoproterozoic|Age: <1330Ma. Sandstone; micaceous siltstone, and shale.||Salvation Group||||25-NOV-13
4597|Coonabildie Formation|69091|6|Mentioned|p202|||Salvation Basin. Age: late Mesoproterozoic|||||Siliciclastic sedimentary rocks.|
4597|Coonabildie Formation|71169|5|Briefly described|p80|Ectasian|Calymmian|Ward and Oldham Inliers. Deposited in a deltaic to shallow marine setting; paleocurrents from east and north.|1410-1279 Ma|||||
4597|Coonabildie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale, chert, siltstone|
4597|Coonabildie Formation|71269|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Salvation Group.|||Siltstone, lithic fine sandstone, micaceous siltstone, shale. Ripple marks common. Minor medium to coarse sandstone; varicoloured chert. Minor carbonate and conglomerate.|
4597|Coonabildie Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Salvation Basin. ||Salvation Group|||Sandstone, micaceous siltstone and shale.|
4607|Coondoon Formation|23594|6|Mentioned|p20|||||||||
4607|Coondoon Formation|41669|2|Defined|Table 5|Precambrian?||Fully described P36||||||
4607|Coondoon Formation|43055|3|Fully described|Table 5, Table 4|||of Manganese Group||||||
4607|Coondoon Formation|43056|5|Briefly described|Map Legend|||of Manganese Group||||||22-DEC-09
4607|Coondoon Formation|44142|4|Described|p311, p316 Tb.4-4, p322-323|||1-100m thick deposits in fluviatile, closed and barred basins with later marine transgressions. Base of Manganese Subgroup in Central BALFOUR DOWNS. Coeval with Woblegun Formation. Deposited on paleokarst topography formed on Carawine Dolomite and Pinjian Chert Breccia. Includes "Bee Hill Sandstone" of de la Hunty (1963).|1.05 Ga (glauconite K-Ar; Goode and Hall, 1981)|Manganese Subgroup||Unconformably overlies Fortescue and Hamersley Groups. Overlain disconformably by Balfour Formation.|Sandstone, conglomerate, wacke, glauconitic sandstone, shale; minor dolomite.|13-MAR-18
4607|Coondoon Formation|65829|6|Mentioned|p27.|Mesoproterozoic|Mesoproterozoic|Contains glauconitic sandstone towards the top of its succession.||Basal unit in Manganese Group.||||
4607|Coondoon Formation|67183|4|Described|p643, 645, 647-649, 653, 656, 659, 662 |Mesoproterozoic|Mesoproterozoic|Present in the Oakover Basin at base of Manganese Subgroup.Thickness <150m. K-Ar date of 1050 Ma is thought to relate to the intrusion of the Davis Dolerite and is thus considered a minimum age. Note: sandstone at Bee Hill reassigned from Coondoon to Stag Hill Formation|1050 Ma glauconite K-Ar (Goode and Hall 1981) |Base of Manganese Subgroup||Unconformably overlies the Mount Bruce Supergroup, Carawine Dolomite, and granite-greenstones of the Pilbara Craton; unconformably overlain by Stag Arrow Formation.|<150m thick, conglomerate and sedimentary breccia (matrix dominated mass flows) grading to poorly sorted ferruginous sandstone and siltstone,.|
4607|Coondoon Formation|71042|5|Briefly described|p66 fig 2, p67-p68|Mesoproterozoic|Mesoproterozoic|Oakover Basin. This unit is <150m thick. Age from glauconite is interpreted here as a minimum age for the intrusion by the Davis Dolerite. Hosts the primary Maganese orebody at the Oregon Prospect. See also p71, p75-p76, p78-p79, p81. Parts of this unit at Bee Hill reassigned herein to Stag Arrow Formation.|1050 Ma K-Ar Goode & Hall, 1981.|Manganese Group||Equivalent to the Woblegun Formation. Overlain by the Stag Arrow Formation. Overlies the Mount Bruce Supergroup. Unconformably overlies the Carawine Dolomite.|Conglomerate, sedimentary breccia, poorly sorted ferruginous sandstone and siltstone.|24-MAY-19
4607|Coondoon Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, greywacke, crystalline dolostone/dolomite, conglomerate|
4666|Copalcarra Sandstone|37460|6|Mentioned|p178|||||||||
4684|Copper Hills Porphyry|29447|6|Mentioned|p11|||||||||
4684|Copper Hills Porphyry|30488|6|Mentioned|p91|||2880 +/- 66 m.y. Refers De Laeter & Trendall (1970)||||||
4684|Copper Hills Porphyry|30489|4|Described|p97|||Refers Noldart and Wyatt (1963), Compston & Arriers (1968).||||||21-AUG-07
4684|Copper Hills Porphyry|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
4684|Copper Hills Porphyry|35260|6|Mentioned|Fig.12|||||||||
4684|Copper Hills Porphyry|36874|5|Briefly described|p87|||||||||
4684|Copper Hills Porphyry|38510|6|Mentioned|Table 1|||||||||
4684|Copper Hills Porphyry|38514|5|Briefly described|Table II|||||||||
4684|Copper Hills Porphyry|39697|6|Mentioned|p22|||||||||
4684|Copper Hills Porphyry|45923|4|Described|p.108,109|||On many pages. Pl.V, 68,102,13,120.Middle? Achaeozoic. Same as Copper Hills Porphyry Formation. p.9,108.||||||
4684|Copper Hills Porphyry|63441|5|Briefly described|p8 Tb. 2|Archean|Archean|Of Emu Pool Supersuite. Age: 3321+/-4Ma. Geological province: Pilbara Craton.||||||07-FEB-11
4702|Corby Limestone Member|14019|5|Briefly described|p21|Middle Cambrian|Middle Cambrian|Of the Panton Formation (Negri Subgroup, Goose Hole Group).  ||||||
4702|Corby Limestone Member|40993|6|Mentioned|Fig.1|||||||||
4702|Corby Limestone Member|41840|4|Described|p43|||||||||
4702|Corby Limestone Member|41864|4|Described|p19|||||||||
4702|Corby Limestone Member|41865|5|Briefly described|Map legend|Middle Cambrian||||||||
4702|Corby Limestone Member|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
4702|Corby Limestone Member|42070|6|Mentioned|p4|||||||||
4702|Corby Limestone Member|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
4702|Corby Limestone Member|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
4702|Corby Limestone Member|60419|4|Described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Panton Formation. Max. thickness: 4.6 m. Shale, marl, marly limestone and limestone. Fossiliferous. Intertidal to shoreface and shallow subtidal. Contains fauna of Ordian age. Geological Province: Ord Basin.||||||
4702|Corby Limestone Member|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Panton Formation (Negri Subgroup, Goose Hole Group).  Grey, stromatolitic fossiliferous limestone.  Geological Province: Ord Basin.||||||
4702|Corby Limestone Member|62789|5|Briefly described|p133|Cambrian|Cambrian|Ord Basin. Contains Xystridura negrina assemblage of moderate diversity including trilobites, brachiopods, hyoliths, molluscs, adrioasteroid ossicles and a ptychoparioid.||Unit in Panton Formation.||||28-MAR-12
4702|Corby Limestone Member|67860|5|Briefly described|p419 Tb. 4-18|Cambrian|Cambrian|0-4 m thick. Type section details given. Unfossiliferous.||Panton Formation|||Grey micritic limestone with chert nodules.|
4702|Corby Limestone Member|69448|5|Briefly described|p33:2-4; 33:5 Fig.33.7; 33:6, 8|Middle Cambrian|Middle Cambrian|Ord Basin. Intertidal, shoreface and shallow subtidal deposits. 2-4.6m thick.||Panton Formation.|||Microbial limestone, hyolith floatstone and oncoid bioclast limestone.|12-JUL-16
4702|Corby Limestone Member|69673|6|Mentioned|p193|||||||||
4702|Corby Limestone Member|71800|5|Briefly described|p26 fig 3|Cambrian|Cambrian|Ord Basin.||Panton Formation||||
4706|Cordalia Formation|12733|6|Mentioned|p555.|||Northern Merlinleigh Sub-basin. Contains good hydrocarbon source rocks.||||||
4706|Cordalia Formation|14228|5|Briefly described|p8, p18|Permian|Permian|||Basal Wooramel Group||Laterally equivalent in part to Callytharra Formation. Is overlain conformably by Moogooloo Sandstone.|Fine grained, locally silty.|05-OCT-16
4706|Cordalia Formation|23726|5|Briefly described|p45|Early Permian|Early Permian|Overlying unit Moogooloo Sandstone. Underlying unit Callytharra Formation. Geological Province: Carnarvon Basin.||||||
4706|Cordalia Formation|24390|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
4706|Cordalia Formation|42392|6|Mentioned|Fig.1 P114|||Variation of Cordalia Greywacke or Cordalia Sandstone?||||||
4706|Cordalia Formation|50085|5|Briefly described|p19 Fig. 10|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||
4706|Cordalia Formation|61023|5|Briefly described|p34 Fig. 14|Permian|Permian|Geological Province: Southern Carnarvon Basin.||||||11-APR-08
4706|Cordalia Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey claystone?|
4706|Cordalia Formation|67200|5|Briefly described|p7 fig 5, p47, p55, app 2 p5|Sakmarian|Asselian |Thermal conductivity of 1.98 W/mK||Wooramel Group||Unconformably overlain by Moogooloo Sandstone, overlies Callytharra Formation|Interbedded siltstone and limestone with inverterbrate macrofossils.|
4706|Cordalia Formation|67977|5|Briefly described|p481 Fig. 2|Artinskian|Artinskian|Geol. Prov: Merlinleigh Sub-basin, Southern Carnarvon Basin||||is overlain by Moogooloo Sandstone; overlies Callytharra Formation||
4706|Cordalia Formation|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11, Ch3 p23|||Carnarvon Basin. See also Ch3 p35, Ch3 p37, Ch3 p67-p68, Ch3 p73.  ||||||
4706|Cordalia Formation|70774|5|Briefly described|p5 fig 3|Artinskian|Artinskian|Southern Carnarvon Basin.||Wooramel Group||Overlies the Callytharra Formation. Overlain by the Moogooloo Sandstone.||
4706|Cordalia Formation|72910|4|Described|p1, p4-7, p11, 16, 18, p20, p22-24.|Artinskian|Artinskian|Thickness <140m. Interpreted as being deposited in both prodelta and delta front environments. Shown as being part of the Merlinleigh Sub-basin. Type section: Lyndon River, southeast of Winning Homestead, 23d20m50sS, 114d39m30sE. Known only north of the 24d30m parallel of latitude. See also p31-32, p39, p41, p42.||Wooramel Group||Conformably overlies and is partially equivalent to Callytharra Formation. Overlain by Moogooloo Sandstone.|Silty, fine to very fine sandstone, siltstone. Predominantly carbonaceous siltstone in subsurface.|18-FEB-21
4734|Cornelia Sandstone|24183|5|Briefly described|p3 Fig.2|Mesoproterozoic|Mesoproterozoic|Geological Province: Bangemall Basin. Of the Bangemall Group.||||||
4734|Cornelia Sandstone|35596|4|Described|p7|||||||||
4734|Cornelia Sandstone|37022|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early or Middle Proterozoic.||||||10-NOV-14
4734|Cornelia Sandstone|37460|6|Mentioned|p157|||||||||
4734|Cornelia Sandstone|37707|6|Mentioned|Table I|||||||||
4734|Cornelia Sandstone|40089|6|Mentioned|p53|||||||||
4734|Cornelia Sandstone|40355|6|Mentioned|p12|||||||||
4734|Cornelia Sandstone|41360|6|Mentioned|p192|||||||||
4734|Cornelia Sandstone|43492|3|Fully described|8|||||||||
4734|Cornelia Sandstone|44142|4|Described|p309, p310 Tb.4-3, p316 Tb.4-4|||See also p321, p324. Of Brakel and Leech (1979, 1980); here (Williams, 1990) incorporated into Bangemall Group. 5km thick shallow-marine shelf deposits; moderately folded. Resembles Calyie Sandstone and Stag Arrow Formation. Aka Cornelia Inlier.||Bangemall Group||Overlain unconformably, and surrounded, by Savory Group. Correlated with Collier Subgroup.|Mainly quartz sandstone, some glauconitic sandstone; minor shale, siltstone, granule conglomerate.|13-MAR-18
4734|Cornelia Sandstone|50188|1|Redefined|p9-12|Mesoproterozoic|Paleoproterozoic|Of Brakel and Leach (1980)and superseded by Cornelia Fm. now reinstated as C.Sandstone. Geol.Prov: Oldham Inlier. Max. thickness: 2000m+. Unconformable under Skates Hills Formation; conformable under Quadrio Formation. Age: c.1600Ma.||||||07-NOV-08
4734|Cornelia Sandstone|62453|6|Mentioned|p20 Fig. 10|Mesoproterozoic|Mesoproterozoic|Underlies: Browne Formation.||||||
4734|Cornelia Sandstone|63022|5|Briefly described|p1015, p1016 Fig. 2|Mesoproterozoic|Mesoproterozoic|Overlain by Buldya Group. Geological Province: Officer Basin.||||||28-JUL-08
4734|Cornelia Sandstone|64283|1|Redefined|p51, p52|Mesoproterozoic|Paleoproterozoic|Revised/supersedes the "Cornelia Sandstone" + later Cornelia Formation (Williams 1992) as one of 3 distinct former units previously of Cornelia Fm. Name is restricted to steeply dipping sandstone intervals north of Oldham Range. Geol.prov:Oldham Inlier.||||||07-FEB-11
4734|Cornelia Sandstone|64286|5|Briefly described|p72, p73 Fig. 1|||Of Brakel and Leech (1980) and Muhling and Brakel (1985). Revised stratigraphy divided this into Oldham Sandstone, Quadrio Formation and a redefined, more restricted Cornelia Formation.  Geological province: Oldham Inlier. Intensely silicified sandstone.||||||09-MAY-11
4734|Cornelia Sandstone|64580|4|Described|map legend||Mesoproterozoic|Shale, siltstone, chert, and minor sandstone; quartz sandstone to quartzite, and minor siltstone.||||||09-DEC-08
4734|Cornelia Sandstone|64772|5|Briefly described|p13, Plate 1 legend|Proterozoic|Proterozoic|Initially mapped by Brakel and Leech(1980) or Cornelia Formation by Williams (1992, 1995a); later subdivided by Hocking et al 92000a,b) into Oldham Sandstone, Quadrio Formation and Cornelia Sandstone. Age: <1670Ma. Part of Oldham Inlier. See also p34 Fig.22, p50 Fig.37, p82 App.4 Tb.4.5.||||May correlate with Scorpion Group|With Quadrio Formation lithology is: shale, siltstone, chert, and minor sandstone; quartz sandstone to quartzite, and minor siltstone|25-NOV-13
4734|Cornelia Sandstone|65363|5|Briefly described|p5, p6 Fig.5, p11.|||Age is poorly constrained; probably Mesoproterozoic. Forms much of the Oldham Inlier, and underlies the Officer Basin succession in the northwest. Porosity and permeability are briefly discussed.|||||Bluish-grey, pebbly, clayey, medium-grained, cross-bedded feldspathic and micaceous sandstone, moderately sorted, some coarse and granular horizons.|
4734|Cornelia Sandstone|65364|5|Briefly described|p81|||?Mesoproterozoic.|||||Blueish-grey, pebbly, clayey, medium grained, cross-bedded sandstone, well cemented.|16-MAR-12
4734|Cornelia Sandstone|65366|5|Briefly described|p21|||Tentatively identified in GSWA Lancer 1 from 1478.1 - 1501.2 m (base)||||||
4734|Cornelia Sandstone|65371|5|Briefly described|p54 Fig. 1|||Unconformably overlain by Browne Formation, Buldya Group. Pebbly dirty sandstone. Probably fluvial ||||||
4734|Cornelia Sandstone|66107|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Eastern Capricorn Orogen.||||Possible correlative of Collier Group.||
4734|Cornelia Sandstone|67195|6|Mentioned|p19 table 1, p40, p42, 48|Mesoproterozoic|Mesoproterozoic|Thermal conductivity of 3.50 W/mK. Basal unit of one well in this study. See also App 1.|||||Sandstone, mudstone, siltstone.|
4734|Cornelia Sandstone|69091|5|Briefly described|p34||Mesoproterozoic|In GSWA Lancer 1, quartzite below the Officer Basin (1478.9 m to 1501.2 m, TD) was assigned to the Cornelia Sandstone (Haines et al., 2004). Detrital zircons dated by SHRIMP, provided maximum depositional ages of 1305 +/- 14 Ma (GSWA Lancer 1, sandstone, 1490 m depth) and 1279 +/- 25 Ma in outcrop (Bodorkos et al., 2006; Wingate and Bodorkos, 2007).|max dep. 1305+/-14 Ma, 1279+/-25 Ma SHRIMP zircon||||Sandstone.|
4734|Cornelia Sandstone|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Eastern Capricorn Orogen.||||||
4734|Cornelia Sandstone|70936|6|Mentioned|p74|||Intersected at the bottom of Lancer-1 drillhole below thick Neoproterozoic succession,~ 600km SSE of Y10 pit.||||||
4734|Cornelia Sandstone|71169|5|Briefly described|p80|Ectasian|Calymmian|Ward and Oldham Inliers. Deposited in a deltaic to shallow marine setting; paleocurrents from east and north.|1410-1279 Ma|||||
4734|Cornelia Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, mudstone, greensand, sandstone|
4734|Cornelia Sandstone|72034|6|Mentioned|500k_interpgeop16_lut|Mesoproterozoic|Paleoproterozoic|Paterson Orogen. Informally grouped with Quadrio Formation. |Max age 1845+/-62 Ma, Min~1070 Ma.||||Combined description: Shale, siltstone, chert, and minor sandstone; quartz sandstone to quartzite, and minor siltstone.|
4757|Corsair metaserpentinites|32269|6|Mentioned|p313|||||||||
4797|Cowarna Monzogranite|42741|5|Briefly described|map legend|Archean||||||||07-NOV-08
4797|Cowarna Monzogranite|43075|5|Briefly described|p9|||||||||
4797|Cowarna Monzogranite|44202|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
4797|Cowarna Monzogranite|60076|5|Briefly described|p23, p45 App. 1|Archean|Archean|[Agmco]   Leucocratic, medium-grained, biotite bearing monzogranite; contains large phenocrysts of K-feldspar.||||||07-NOV-08
4797|Cowarna Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium-grained, leucocratic, biotite-bearing monzogranite; K-feldspar phenocrysts.||||||07-FEB-11
4797|Cowarna Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained, leucocratic, biotite-bearing monzogranite; K-feldspar phenocrysts.|05-AUG-15
4797|Cowarna Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained, leucocratic, biotite-bearing monzogranite; K-feldspar phenocrysts.|
4797|Cowarna Monzogranite|71270|4|Described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton.|||||Medium-grained, leucocratic, biotite-bearing monzogranite; K-feldspar phenocrysts|
4826|Coyango Greywacke|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Of the Lyons Group. Underlying unit: Austin Formation. Overlying unit: Dumbardo Siltstone.||||||18-APR-05
4826|Coyango Greywacke|32648|6|Mentioned|p32|||Lyons Gp.||||||
4826|Coyango Greywacke|36890|6|Mentioned|p279|||||||||
4826|Coyango Greywacke|37295|6|Mentioned|Table 2|||||||||
4826|Coyango Greywacke|41271|6|Mentioned|p65|||||||||
4826|Coyango Greywacke|44344|14|Not recorded|p.5-7,19,22,24|||O/lies Austin Formation, u/lies Dumbardo Siltstone. (G50-1). opp.4; map.||||||
4826|Coyango Greywacke|44345|14|Not recorded|map legend||Sakmarian|||||||
4826|Coyango Greywacke|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
4826|Coyango Greywacke|45016|2|Defined|p.27-31||Sakmarian|Tb, p7,9,12,13,15,16,22,23,24,26,Fig.48,50,p35,36,39,148. (F50-13-type area).||||||
4826|Coyango Greywacke|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
4875|Credo Granodiorite|22534|5|Briefly described|p11|||||||||
4875|Credo Granodiorite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
4875|Credo Granodiorite|41786|6|Mentioned|Table 2|||Reserved as Credo Granite||||||
4875|Credo Granodiorite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
4875|Credo Granodiorite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
4875|Credo Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggcr]  Medium-grained biotite granodiorite.||||||13-APR-05
4875|Credo Granodiorite|65204|6|Mentioned|p17 Tbl.2.|Neoarchean||0.1-4mm grains; seriate to porphyritic ||||||
4875|Credo Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium-grained biotite granodiorite; foliation strong near margins.||||||07-FEB-11
4875|Credo Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained biotite granodiorite; domal within regional anticline; foliation strongest near margins.|05-AUG-15
4875|Credo Granodiorite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained biotite granodiorite; domal within regional anticline; foliation strongest near margins.|
4875|Credo Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
4875|Credo Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Medium-grained biotite granodiorite; domal within regional anticline; foliation strongest near margins|
4951|Crowhurst Group|22716|5|Briefly described|table4, p236|Mesoproterozoic|Mesoproterozoic|May be equivalent to part of the Birrindudu Group.||||||
4951|Crowhurst Group|23383|6|Mentioned|p20|||Unconformably overlain by Louisa Downs Group on MOUNT RAMSAY.||||||25-JAN-05
4951|Crowhurst Group|23599|6|Mentioned|p16|||Overlying unit Louisa Downs Group||||||
4951|Crowhurst Group|30892|6|Mentioned|Table 1|||Carpentarian age||||||
4951|Crowhurst Group|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
4951|Crowhurst Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
4951|Crowhurst Group|32660|4|Described|Table 3|||||||||
4951|Crowhurst Group|32728|6|Mentioned|Fig.3|||||||||
4951|Crowhurst Group|36551|6|Mentioned|Table 10|||||||||
4951|Crowhurst Group|36885|4|Described|p183|||||||||
4951|Crowhurst Group|37462|4|Described|Table4.III|||||||||
4951|Crowhurst Group|38243|6|Mentioned|p353|||||||||
4951|Crowhurst Group|38988|6|Mentioned|Fig.4|||||||||
4951|Crowhurst Group|41987|6|Mentioned|p73|||||||||
4951|Crowhurst Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
4951|Crowhurst Group|43595|5|Briefly described|p443|||||||||
4951|Crowhurst Group|44140|4|Described|p293-294, p296 fig 4-3, p299|Paleoproterozoic|Paleoproterozoic|Roberts et al. (1968). Locally restricted. About 150 m thick. Divided into 4 conformable units.|>1762 +/- 15 Ma.||Includes Hilfordy Formation, Liga Shale, Collett Siltstone and Hibberson Dolomite.|Conformably overlies Kimberley Group. Overlain by Colombo Sandstone unconformably. Regarded as equivalent to Bastion Group.|Dolomite with stromatolites, purple and green shale, siltstone and sandstone.|07-MAR-18
4951|Crowhurst Group|44155|6|Mentioned|p251 Tb.3-11, p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|||||Is overlain unconformably by Harms Sandstone.||
4951|Crowhurst Group|44231|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes the Hilfordy Formation, Liga Shale, Collett Siltstone and Hibberson Dolomite. Age: c.?1500Ma. Geological Basin: Crowhurst Basin.||||||26-MAY-05
4951|Crowhurst Group|44397|14|Not recorded|p.9,19, Table 2||Carpentarian|Defn. on Tech.File E/52-9.||||||
4951|Crowhurst Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
4951|Crowhurst Group|45047|5|Briefly described|p28|||Carpentarian||||||
4951|Crowhurst Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Kimberley Basin.||||||07-FEB-11
4951|Crowhurst Group|60724|6|Mentioned|p5 Fig. 2|||||||||
4951|Crowhurst Group|61574|5|Briefly described|p690|Proterozoic|Proterozoic|Includes the Hilfordy Formation and Liga Shale. Overlain unconformably by the Yurabi and Egan Formations.||||||07-JAN-10
4951|Crowhurst Group|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|[This article changes the age of a number of units, including this one, without explanation. Error in Figure 10?]|||Includes Hibberson Dolomite.|||19-MAY-15
4951|Crowhurst Group|64580|4|Described|map legend|Mesoproterozoic|Mesoproterozoic|Siltstone, shale, dolomite, stromatolitic dolomite, and sandstone.||||||28-SEP-12
4951|Crowhurst Group|68244|6|Mentioned|p666|Mesoproterozoic|Mesoproterozoic|||||Overlain unconformably by Louisa Downs Group.||
4951|Crowhurst Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
4951|Crowhurst Group|69099|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic||||||Siltstone, shale, dolomite, stromatolitic dolomite, and sandstone.|03-APR-19
4951|Crowhurst Group|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Mesoproterozoic||||||Undivided; siltstone, shale, dolomite, stromatolitic dolomite and sandstone.|
4951|Crowhurst Group|69587|6|Mentioned|2_5m_geologyp98_lut.csv|||||||||
4951|Crowhurst Group|69597|6|Mentioned|p5 fig 2b|||||||||
4951|Crowhurst Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Paleoproterozoic||||||Undivided, siltstone, shale, dolomite, stromatolitic dolomite, and sandstone|
4951|Crowhurst Group|70154|6|Mentioned|2_5m_geologyp98_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Siltstone, shale, dolomite, stromatolitic dolomite and sandstone.|
4951|Crowhurst Group|70731|6|Mentioned|p268|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
4951|Crowhurst Group|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Crowhurst Basin.||||||
4951|Crowhurst Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1797-1640 Ma (inferred)||Includes Collett Siltstone, Hibberson Dolomite, Hilfordy Formation, Liga Shale.||Siltstone, shale, dolomite, stromatolitic dolomite, and sandstone.|
4951|Crowhurst Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Crowhurst Basin.|||||Siltstone, shale, dolomite, stromatolitic dolomite, and sandstone.|
4952|Crown Basalt|31042|6|Mentioned|Fig. 4|||Correlation||||||
4952|Crown Basalt|43162|6|Mentioned|6|||||||||
4952|Crown Basalt|45543|4|Described|p,102,105. Fig.2||Archean|Unit of Woolyeenyer Group.||||||07-NOV-08
4964|Croydon Group|61253|5|Briefly described|p56, p52 Fig. 2|Archean|Archean|Of De Grey Supergroup. Consists largely of siliciclastic rocks of Constantine Sandstone and Mallina Formation.  Overlies Bookingarra Group.  Age: c.2.95-2.94Ga (Smithies et al, 1999, 2001). Geological Province: Pilbara Craton/Mallina Basin.||||||07-NOV-08
4964|Croydon Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Supergroup. Includes Lalla Rookh Sandstone, Bookingarra Formation, Constantine Sandstone, Kialrah Rhyolite and Mallina Formation.  Ages: c.2948Ma and c.2941Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
4964|Croydon Group|63441|2|Defined|p5 Tb. 1, p27|Archean|Archean|Of De Grey Supergp. Comprises Bookingarra, Cattle Well, Mallina Fms, Constantine Sst, Rushall Slate and Cistern Fm. Age: 2970-2930Ma. Coarse- to fine-grained siliciclastic sedimentary rocks, lesser mafic+felsic volcanic rock. Geol.prov: Mallina Basin.||||||07-FEB-11
4964|Croydon Group|63538|4|Described|p2 Fig. 1, p7, p10, p16, p17, p32-33|Archean|Archean|Of De Grey Supergroup. Includes 4 or 5 formations. Underlain disconformably by Whim Creek Group. Overlain by Louden Volcanics, Mount Negri Volcanics. Age: 2970-2930 Ma. Geological Province: De Grey Superbasin. Coarse- to fine-grained siliciclastic sedimentary rocks.||||||19-APR-13
4964|Croydon Group|64174|5|Briefly described|Map legend|Archean|Archean|Of the De Grey Supergroup. Includes Cistern, Formation, Rushall Slate, Bookingarra Formation, Kialrah Rhyolite, Mallina Formation and Constantine Sandstone.  Age range: <2964Ma - 2943Ma. Geological province: Mallina Basin.||||||07-NOV-08
4964|Croydon Group|64580|4|Described|map legend||Mesoarchean|Dacite tuff, tuffaceous siltstone, sandstone, siltstone,  shale, wacke, conglomerate, and carbonate rock; weakly metamorphosed.||||||14-OCT-08
4964|Croydon Group|64621|5|Briefly described|Map legend|Archean|Archean|Of De Grey Supergroup. Includes Lalla Rookh Sandstone. Comprehensive lithological details included.||||||07-NOV-08
4964|Croydon Group|64632|5|Briefly described|p201 Fig.1, p203, p205|Mesoarchean|Mesoarchean|Main fill of Mallina Basin. Composition of basalts influenced by subduction|2970-2930 Ma|Of the De Grey Supergroup.|Includes Bookingarra Formation||The main sedimentary package includes sandstone, siltstone, and conglomerate deposited on a series of submarine fans.|
4964|Croydon Group|66108|5|Briefly described|Map legend|Mesoarchean|Mesoarchean|Unit of De Grey Supergroup. Includes Mallina Formation and Lalla Rookh Sandstone.||||||
4964|Croydon Group|66118|4|Described|p146-150, p153 Fig.7, p157, p158 Tb.2|||Pilbara Craton. Mallina Basin.|2970-2940 or 2990 Ma, 2960-2930 Ma|De Grey Supergroup||Unconformably overlies Whim Creek Group. Unconformably overlies rocks in the southeastern part of Pilbara Well greenstone belt.|Low-grade clastic sedimentary rocks. Conglomerate and sandstone; subarkose, wacke, shale.|
4964|Croydon Group|66122|5|Briefly described|p75|Archean|Archean|Mount Goldsworthy area, NE Pilbara Craton.|||Constantine Sandstone.|||
4964|Croydon Group|66217|4|Described|p1, p6 Table 1, p9, pp38-42. |Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins, East Pilbara Terrane, Pilbara Craton. Tilted by the c.2905 Ma Mosquito Creek Orogeny. Hosts shear-zone hosted, epigenetic and epithermal gold deposits.|2970-2940 Ma.|Unit in De Grey Supergroup.|Includes Lalla Rookh and Constantine Sandstones; Rushall Slate; Bookingarra, Cistern, Cattle Well Formations, and Kialrah Rhyolite.|Unconformably overlies Gorge Creek Group. Is overlain unconformably by the Fortescue Group.|Mainly coarse- to fine-grained clastic sedimentary rocks (turbidites), with mafic and felsic volcanic rocks.|
4964|Croydon Group|66745|6|Mentioned|p50 Fig.1.|Mesoarchean|Mesoarchean|||Unit in De Grey Supergroup.||||
4964|Croydon Group|67130|6|Mentioned|p13|||||De Grey Supergroup||||
4964|Croydon Group|67197|5|Briefly described|p5, p9, p14, p19, p22, p25, p33-34, p36|||De Grey Superbasin.|2970-2930 Ma.|De Grey Supergroup.|Lalla Rookh Sandstone.|Unconformably overlies Gorge Creek Group.||
4964|Croydon Group|67201|4|Described|p7, p12, p13 Fig.8, p16-17, see comments|||In northwestern Pilbara Craton, unconformably overlies West Pilbara Superterrane and East Pilbara Terrane. De Grey Superbasin, Mallina Basin and Whim Creek greenstone belt. Max. depositional age (Mallina Formation and Constantine Sandstone): 2994+/-4 Ma, although xenocrystic zircons from intruding granites indicate a more realistic max age of c. 2970 Ma (Smithies et al. 2001). Tight to isoclinal folding. Page location continued: p20-23, p57, p59-60, p63-64.|2970-2930 Ma|De Grey Supergroup|Mallina Formation, Kialrah Rhyolite, Bookingarra Formation, Constantine Sandstone, Rushall Slate, Cistern Formation, Lalla Rookh Sandstone, Cattle Well Formation, Coonieena Basalt|Unconformable over Whim Creek Group.|Sedimentary and volcanic.|22-NOV-16
4964|Croydon Group|67269|6|Mentioned|p5|Paleoarchean|Paleoarchean||||Lalla Rookh Sandstone.|||
4964|Croydon Group|68035|5|Briefly described|p291, 294, p286 Fig 3, p290 Fig 5|Mesoarchean|Mesoarchean|Mallina Basin, De Grey Superbasin. Includes VHMS and sediment-hosted Pb-Zn and Cu deposits at several localities.|2970 - 2940 Ma||Includes Bookingarra Formation, Constantine Sandstone and Mallina Formation.|||
4964|Croydon Group|68280|6|Mentioned|p3|||||||||
4964|Croydon Group|68281|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Lalla Rookh and Mallina Basins, De Grey Superbasin, Pilbara Craton.||Of the De Grey Supergroup.|Includes Lalla Rookh Sandstone, Mallina Formation.|||11-JUN-14
4964|Croydon Group|68282|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Lalla Rookh Basin, De Grey Superbasin.||Of the De Grey Supergroup|Includes Lalla Rookh Sandstone.|||03-DEC-14
4964|Croydon Group|68283|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina and Lalla Rookh Basins.|< 3020 Ma|Of the De Grey Supergroup.|Includes Mallina Formation, Kialrah Rhyolite, Constantine Sandstone, Bookingarra Formation, Lalla Rookh Sandstone.|||
4964|Croydon Group|69013|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Mallina Basin. Age constrained by the De Grey Supergroup.|3022-3016 Ma|Of the De Grey Supergroup.|Includes the Mallina Formation.||Includes siliciclastic sedimentary rocks containing layers of porphyritic dacite; metamorphosed.|30-APR-14
4964|Croydon Group|69015|5|Briefly described|Map Legend|Mesoarchean|Mesoarchean|Lalla Rookh Basin, De Grey Superbasin.||Of the De Grey Supergroup.|Includes the Lalla Rookh Sandstone.|||05-MAY-14
4964|Croydon Group|69167|4|Described|geologyp_lut.csv|Mesoarchean|Mesoarchean|||De Grey Supergroup|Includes Kialrah Rhyolite, Mallina Formation, Lalla Rookh Sandstone, Cattle Well Formation, Constantine Sandstone||Ferruginous siltstone, shale, and iron formation; metamorphosed. Wacke; locally subarkosic; fine to coarse grained; well developed graded units; minor pebble beds and shale.|
4964|Croydon Group|69185|4|Described|500k_geologyp08_lut.csv|||Geological Province: Pilbara Craton.||Unit of De Grey Supergroup.|Includes Bookingarra Formation, Cistern Formation, Constantine Sandstone, Kialrah Rhyolite, Lalla Rookh Sandstone, Mallina Formation, Rushall Slate.||Basalt and local hyaloclastic breccia; metamorphosed; coarse-grained wacke, dacite tuff, tuffaceous and laminated siltstone and shale, sandstone, siltstone, carbonate rock; metamorphosed; sub-arkosic wacke; metamorphosed.|
4964|Croydon Group|69301|4|Described|p5-6, p9 Tb.1, p14-15, p20-21|||Pilbara Craton. West Pilbara Superterrane. Mallina Basin.|2980-2940 Ma from unit ages|De Grey Supergroup|Kialrah Rhyolite, Lalla Rookh Sandstone, Bookingarra Formation, Rushall Slate, Cistern Formation, Mallina Formation, Constantine Sandstone, Cattle Well Formation, Coonieena Basalt|Regional unconformity between overlying Gorge Creek Group and underlying Whundo Group.||
4964|Croydon Group|69590|4|Described|GEOL_LUT_CSV files|Mesoarchean|Mesoarchean|Geological province: Pilbara Craton. Of De Grey Superbasin. Events: North Pilbara Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|3015-2931 Ma (inferred)|Unit of De Grey Supergroup.|Includes Bookingarra Formation, Cattle Well Formation, Constantine Sandstone, Kialrah Rhyolite, Lalla Rookh Sandstone, Mallina Formation, South Mallina Basalt Member.||Wacke; locally subarkosic; fine- to coarse-grained; well developed graded units; minor pebble beds and shale; turbiditic; metamorphosed, basalt, dacitic tuffs.|
4964|Croydon Group|70022|5|Briefly described|p113-116|||Mallina Basin, Pilbara Craton.|3015-2930 Ma.|De Grey Supergroup.|Constantine, Lalla Rookh Sandstones; Mallina, Cattle Well Formations; Coonieena Basalt.|Unconformably overlies Gorge Creek Group.||
4964|Croydon Group|70775|4|Described|iii, p11-p13, p38-p41|Mesoarchean||Mallina Basin. The authors note that this group should in future be subdivided into at least three groups on the basis of its exceptional time span (3015-2931 Ma), the existence of a regional unconformity at c.2955 Ma and identification of four deformation events. The authors however, do not go as far as revising this group and this remains simply a recommendation on their part. See also p43-p47, p50, p54-p57, p65, p70, p74, p81, p94-p95, p100.|< 2990 Ma||Includes the Constantine Sandstone, Mallina Formation, Lalla Rookh Sandstone and the Cattle Well Formation.|Overlies the Cleaverville Formation. Overlies the Gorge Creek Group. Faulted against the Bookingarra Group. Overlain by the Nullagine Group. Intruded by the Indee Suite.|Alternating sandstone, iron-rich shale, banded iron formation and chert.|
4964|Croydon Group|71041|6|Mentioned|p45 fig 2, p56|||In DeGrey Superbasin. Includes metabasalts.|||Includes the Mallina Formation.|Overlies the Gorge Creek Group.||08-NOV-17
4964|Croydon Group|71137|6|Mentioned|p2, 5|Archean|Archean||||Lalla Rookh Formation, Constantine Sandstone.|Unconformably overlies Gorge Creek Group.||
4964|Croydon Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, banded iron formation, conglomerate, silstone|
4964|Croydon Group|71349|6|Mentioned|p738|||Extensive sedimentary sequence. Resulted from c.3.2 Ga rifting of the Pilbara.||||||
4964|Croydon Group|72034|6|Mentioned|500k_interpgeop16_lut|Mesoarchean|Mesoarchean|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Kialrah Rhyolite, Rushall Slate, Cistern Formation, Mallina Formation, Constantine Sandstone, Lalla Rookh Sandstone, Cattle Well Formation.|||
4964|Croydon Group|72251|5|Briefly described|p52,54|Mesoarchean|Mesoarchean|Geological province: East Pilbara Terrane and West Pilbara Superterrane, Pilbara Craton. Of De Grey Superbasin.|3051-2930 Ma|Unit of De Grey Supergroup.|Includes Lalla Rookh and Cattle Well formations, and Constantine Sandstone.|Overlain by, and correlable to Bookingarra Group. Correlable to Whim Creek Group. Underlain unconformably by Gorge Creek Group.||
4964|Croydon Group|72668|4|Described|p3-4, p7-8, p12-15, p21-22, p24, p28|||Forms the main fill of the Mallina and the Lalla Rookh basins. Has been redefined to incorporate the former Bookingarra Group. Sedimentary rocks are interpreted to have been deposited in a series of submarine fans. Deposited during long lived extension following the collision of the WPS and EP. Detritral zircon age patterns are similar to a mixture of EP and WPS crust. Rhyolite flows in the upper part of the group are 2948 +/- 3 Ma (GSWA, 2006). Gravity modelling indicates a preserved thickness of no more than ~5km. Hosts VMS mineralisation in addition to the Whim Creek Group.|c. 2970-2930 Ma|De Grey Supergroup|Includes the Mallina Formation, Constantine Sandstone, Cattle Well Formation, Lalla Rookh Sandstone, Bookingarra Formation.|Disconformably overlies the Whim Creek Group. Unconformably overlain by the Fortescue Group.|Siliciclastic sedimentary rock, including sandstone, siltstone and conglomerate in addition to boninite like rocks and gabbroic intrusions. Rhyolite also present.|13-JAN-22
4964|Croydon Group|73598|6|Mentioned|p1212|Mesoarchean|Mesoarchean|East Pilbara Terrane.||De Grey Supergroup.|Cattle Well Formation, Lalla Rookh Sandstone.|Unconformably overlies Gorge Creek Group.||
5007|Cumberdale chert|29573|6|Mentioned|p84|||||||||
5020|Cummins Range carbonatite|505|4|Described|p711-713|Proterozoic|Proterozoic|Halls Creek Province. U-Pb zircon age; also 905 +/- 2 Ma (Rb-Sr phlogopite-whole rock and phlogopite-apatite separates) by Sun, Jaques and McCulloch (1986), and 854 +/- 57 Ma (K-Ar on pyroxenes from Cummins Range). Contains an uneconomic (as at 1990) inferred resource of 3 to 4 Mt at 2-4% Rare Earth Oxides within 80m of the surface, including 50-100 ppm Eu2O3. Suggested genesis was a cold intrusion from mantle sources.|1012 +/- 12 Ma (Pidgeon, Smith and Fanning, 1986)|||Intrudes rocks correlated with Olympio Fm, Halls Creek Group.|Plug of calcite-dominant (sovite) and dolomite-dominant (beforsite) carbonatite phases; a weathered capping of silicified, limonitic collapse breccia; all enclosed by an envelope of carbonated, mica-rich pyroxenite, largely altered to amphibolite.|10-NOV-14
5020|Cummins Range carbonatite|22716|5|Briefly described|p238|Tonian|Tonian|Age: approx. 900Ma||||||
5020|Cummins Range carbonatite|22754|5|Briefly described|p22|Tonian|Tonian|Age: 905 Ma.||||||
5020|Cummins Range carbonatite|41158|6|Mentioned|p65|||||||||
5020|Cummins Range carbonatite|64329|6|Mentioned|p27 Tb. 7|||Presented as a selected thorium deposit.||||||
5027|Cundlego Formation|14228|6|Mentioned|p8|Kungurian|Kungurian|||Byro Group||||
5027|Cundlego Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
5027|Cundlego Formation|23311|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
5027|Cundlego Formation|23312|5|Briefly described|map legend|Artinskian|Artinskian|Of Byro Group.||||||
5027|Cundlego Formation|23403|4|Described|p8|Early Permian|Early Permian|Of Byro Group.||||||24-NOV-09
5027|Cundlego Formation|23726|5|Briefly described|p58|Early Permian|Early Permian|Of Byro Group. Overlying unit Quinnanie Shale. Underlying unit Bulgadoo Shale. Geological Province: Carnarvon Basin.||||||
5027|Cundlego Formation|23815|4|Described|p286|Artinskian|Artinskian|Geological Province: Merlinleigh Sub-basin. Of the Minilya Subgroup. Overlying unit: Quinnanie Shale and Wandagee Formation (conformable). Underlying unit: Bulgadoo Shale (conformable). Max. thickness: 412 m. Marine fossils are present.||||||02-MAY-07
5027|Cundlego Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Byro Group.||||||
5027|Cundlego Formation|30449|6|Mentioned|p11|||Brachiopods. [Originally entered for Qld. CEBMar95]||||||
5027|Cundlego Formation|30545|6|Mentioned|Fig.2|||Artinskian||||||
5027|Cundlego Formation|32648|6|Mentioned|p32|||Byro Gp.||||||
5027|Cundlego Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
5027|Cundlego Formation|33710|6|Mentioned|Fig.1|||||||||
5027|Cundlego Formation|34532|6|Mentioned|p225|||See also P226. Byro Gp.||||||
5027|Cundlego Formation|35282|6|Mentioned|Fig.30|||||||||
5027|Cundlego Formation|36020|6|Mentioned|p392|||||||||
5027|Cundlego Formation|36257|6|Mentioned|Table 2.1|||||||||
5027|Cundlego Formation|36387|6|Mentioned|p186|||||||||
5027|Cundlego Formation|36890|3|Fully described|p286|||Formerly Cundlego Series||||||
5027|Cundlego Formation|37295|6|Mentioned|p54|||||||||
5027|Cundlego Formation|37304|6|Mentioned|p55|||||||||
5027|Cundlego Formation|37312|6|Mentioned|p11|||||||||
5027|Cundlego Formation|37549|6|Mentioned|p122|||||||||
5027|Cundlego Formation|39316|6|Mentioned|Fig.2|||||||||
5027|Cundlego Formation|39615|6|Mentioned|p90|||||||||
5027|Cundlego Formation|39974|6|Mentioned|p113|||||||||
5027|Cundlego Formation|40617|6|Mentioned|Fig.1|||||||||
5027|Cundlego Formation|41049|6|Mentioned|p37|||||||||
5027|Cundlego Formation|41071|6|Mentioned|p25|||||||||
5027|Cundlego Formation|41271|3|Fully described|p96|||||||||
5027|Cundlego Formation|41438|6|Mentioned|Fig.11|||||||||
5027|Cundlego Formation|42116|5|Briefly described|p43|||See also Fig.17||||||
5027|Cundlego Formation|42392|5|Briefly described|p118|||Byro Group||||||
5027|Cundlego Formation|42540|6|Mentioned|Table 2 P314|||||||||
5027|Cundlego Formation|42654|6|Mentioned|p12|||||||||
5027|Cundlego Formation|42994|6|Mentioned|p40|||Also p78.||||||
5027|Cundlego Formation|43015|5|Briefly described|Table 1,p319|||||||||
5027|Cundlego Formation|43737|6|Mentioned|p5||Kungurian|||||||
5027|Cundlego Formation|44219|14|Not recorded|p31||Artinskian|||||||
5027|Cundlego Formation|44344|14|Not recorded|p.12-14, opp.4,map||Artinskian|Artinskian; basal fm of Minilya Subgroup (Byro Group). (G50-1).||||||
5027|Cundlego Formation|44345|14|Not recorded|map legend||Artinskian|||||||
5027|Cundlego Formation|44532|4|Described|p.7,8, map|||(G50-5).||||||
5027|Cundlego Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
5027|Cundlego Formation|44537|14|Not recorded|map legend||Artinskian|||||||
5027|Cundlego Formation|44657|14|Not recorded|p.5,6,9|||||||||
5027|Cundlego Formation|44994|5|Briefly described|Fig.7|||Perm. Correlation. Byro Gp.||||||
5027|Cundlego Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group). Geological Province: Carnarvon Basin.||||||31-MAY-06
5027|Cundlego Formation|45016|2|Defined|p.159-165||Artinskian|Tb, p.92,122,124,125,130,135,138-143,155,144,145,157,166,167,181. (F50-13 type area).||||||
5027|Cundlego Formation|45168|6|Mentioned|p6|||||||||
5027|Cundlego Formation|48610|14|Not recorded|Pl.1|||||||||
5027|Cundlego Formation|48831|14|Not recorded|p.7,21,30,68|||||||||
5027|Cundlego Formation|48848|14|Not recorded|p.67,75,76,83|||||||||
5027|Cundlego Formation|48858|14|Not recorded|p.5-15||Artinskian|Artinskian; deposited in conditions of intermittent turbulence, i.e. delta. (G50-1/Norton). Pl.2.||||||
5027|Cundlego Formation|49644|5|Briefly described|Table|||||||||
5027|Cundlego Formation|60331|5|Briefly described|p33 Fig.2|Kungurian|Kungurian|Of the Byro Group. Overlies Bulgadoo Formation. Overlain by Quinnanie Shale. Geological Province: Southern Carnarvon Basin.||||||
5027|Cundlego Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Minilya Sub-Group (Byro Group).||||||
5027|Cundlego Formation|64580|5|Briefly described|map legend|||Of Middle Byro Group. Interbedded black mudstone, siltstone, and fine-grained sandstone.||||||15-DEC-08
5027|Cundlego Formation|64974|5|Briefly described|p147 Fig. 5|Kungurian|Kungurian|Includes Quinnanie Shale. Geological Province: Carnarvon Basin.||||||24-JUN-09
5027|Cundlego Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey/light grey sandstone, finely laminated, pin stripe laminations; dark brown siltstone/sandstone heavily bioturbated. 50/50|
5027|Cundlego Formation|67200|5|Briefly described|p7 fig 5, p18 table 1|Kungurian|Artinskian|Thermal Conductivity of 2.53 W/mK. See also p47, p54, app 2 p5. ||Byro Group||Overlies Bulgadoo Shale, overlain by Quinnanie Shale, Wandagee Formation|Interbedded siltstone and sandstone with trough cross beds and hummocky cross stratification.|
5027|Cundlego Formation|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.||Of the Byro Group.||Underlain by the Bulgadoo Shale.|Comprises interbedded grey siltstone and fine- to medium-grained sandstone; commonly swaley cross-stratified.|
5027|Cundlego Formation|69028|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin. Mapped with Bulgadoo Shale, Quinnanie Shale and Wandagee Formation as a single unit.||Of the Byro Group.|||Interbedded black mudstone, siltstone and fine-grained sandstone.|06-MAY-14
5027|Cundlego Formation|69166|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian|||Byro Group||||
5027|Cundlego Formation|69182|6|Mentioned|Ch3 p55|||||||Overlies the Bulgadoo Shale.||
5027|Cundlego Formation|69547|5|Briefly described|p193,201|Artinskian|Artinskian|Southern Carnarvon Basin.||Unit of Byro Group.||Underlain by Bulgadoo Shale.||
5027|Cundlego Formation|69583|5|Briefly described|p130, Plate 3.|Permian|Permian|Southern Carnarvon Basin. Mapped as one unit with Bulgadoo Shale.||Byro Group.|||Black shale and siltstone overlain by fine-grained sandstone; hummocky and swaley cross-stratified.|
5027|Cundlego Formation|70795|4|Described|100k_geologyp_lut.csv|Kungurian|Kungurian|Also 100k_interpgeop_lut.csv|283-272 Ma|Byro Group||Grades into Quinnanie Shale|Interbedded grey siltstone and fine- to medium-grained sandstone; commonly swaley cross-stratified.|
5027|Cundlego Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale, greywacke|
5027|Cundlego Formation|72910|4|Described|p10-11, p18, p23, p33, p38-39, p41.|Kungurian|Kungurian|Type section: Minilya River, north of Wandagee Hill, 23d45m30sS, 114d25m00sE. Locally abundant fauna. Said to be Artinskian age p39.||Byro Group||Conformably overlies Bulgadoo Shale and underlies Quinnanie Shale, Wandadgee Formation.|Grey siltstone interbedded with fine to medium sandstone.|
5038|Curbur Formation|23815|6|Mentioned|p281|||Geological Province: Byro Sub-basin. Mapped as the Wooramel Group.||||||
5038|Curbur Formation|36890|6|Mentioned|p281|||||||||
5038|Curbur Formation|37295|6|Mentioned|Table 2|||||||||
5038|Curbur Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
5038|Curbur Formation|45016|2|Defined|p.121-2||Artinskian|Tb, p75,97,115,120.||||||
5038|Curbur Formation|48885|14|Not recorded|p.2||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6).||||||
5038|Curbur Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
5038|Curbur Formation|72910|6|Mentioned|p22.|Artinskian|Artinskian|Byro Sub-basin. Abandoned name, now believed to be, in part, equivalent to the Ballythanna Sandstone Member.||||||
5039|Curdamuda Sandstone|33166|6|Mentioned|p62|||Refers Teichert (1952)||||||
5039|Curdamuda Sandstone|44657|14|Not recorded|p.11|||||||||
5039|Curdamuda Sandstone|44997|14|Not recorded|p41||Oxfordian|Oxfordian rather than Bajoc.||||||
5039|Curdamuda Sandstone|48610|14|Not recorded|Pl.1|||||||||
5139|Dales Gorge Member|22682|5|Briefly described|p30|Siderian|Siderian|2470 +/- 4 Ma. Brockman Supersequence. Overlies Newman sequence.||||||03-MAR-10
5139|Dales Gorge Member|22689|6|Mentioned|138,139|||Geol province Hamersley Basin. Parent Brockman Iron Formation||||||
5139|Dales Gorge Member|22701|4|Described|p40|Siderian|Archean|Brockman Iron Formation, Hamersley Basin. 2490 +/- 20 Ma zircon, 2470 +/- 4 Ma using SHRIMP.||||||07-NOV-08
5139|Dales Gorge Member|23045|5|Briefly described|289|||Parent Hamersley Group||||||
5139|Dales Gorge Member|23046|6|Mentioned|171|||Underlying unit Mount McRae Shale||||||
5139|Dales Gorge Member|23047|6|Mentioned|34|||Of the Brockman Iron Formation. Hamersley Province. .||||||10-FEB-09
5139|Dales Gorge Member|23126|5|Briefly described|p381|||||||||
5139|Dales Gorge Member|23194|5|Briefly described|p41||Pliocene|Deposition occured at ~2.470my. Brockman Iron Formation.||||||
5139|Dales Gorge Member|23354|5|Briefly described|315|||||||||
5139|Dales Gorge Member|23536|4|Described|Fig 2 p 429|||Also see p 432.||||||
5139|Dales Gorge Member|23570|5|Briefly described|p27|||Age: 2490+/-20Ma.   Parent: Brockman Iron Fm.   Geological Province: Pilbara Craton||||||
5139|Dales Gorge Member|23612|5|Briefly described|p840|Archean|Archean|Age: 2470+/-4 Ma (SHRIMP U-Pb zircon). Of Brockman Iron Formation.||||||07-NOV-08
5139|Dales Gorge Member|24041|4|Described|p492|Paleoproterozoic|Archean|Of the Brockman Iron Formation.||||||07-NOV-08
5139|Dales Gorge Member|24231|5|Briefly described|p186 Fig.2|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||
5139|Dales Gorge Member|24426|4|Described|p215|Paleoproterozoic|Archean|Includes banded iron-formation and shale. Thickness: ~145 m. Geological Province: Hamersley Province. Of Brockman Iron Formation. Overlies Mount McRae Shale. Overlain by Whaleback Shale Member.||||||07-FEB-11
5139|Dales Gorge Member|24544|4|Described|p57 Fig.43|Paleoproterozoic|Paleoproterozoic|Of Brockman Iron Formation. Overlies Mount McRae Shale. Overlain by Whaleback Shale Member. Banded iron-formation. Age: 2479 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
5139|Dales Gorge Member|29594|6|Mentioned|p9|||||||||
5139|Dales Gorge Member|29596|3|Fully described|p1216|||||||||
5139|Dales Gorge Member|29629|5|Briefly described|p899|||||||||
5139|Dales Gorge Member|29716|4|Described|Table 1|||||||||
5139|Dales Gorge Member|29717|6|Mentioned|p1154|||||||||
5139|Dales Gorge Member|30437|6|Mentioned|p89|||Bulk of hematite deposits||||||
5139|Dales Gorge Member|30685|5|Briefly described|p907|||Re mineralization||||||
5139|Dales Gorge Member|31021|5|Briefly described|p893|||||||||
5139|Dales Gorge Member|31099|6|Mentioned|p41|||Phosphorus content||||||
5139|Dales Gorge Member|31670|4|Described|p911|||||||||
5139|Dales Gorge Member|31671|5|Briefly described|p11|||||||||
5139|Dales Gorge Member|32144|6|Mentioned|p116|||Organic matter||||||
5139|Dales Gorge Member|32326|4|Described|p122|||Refers Trendall & Blockley (1968)||||||
5139|Dales Gorge Member|33538|6|Mentioned|p291|||||||||
5139|Dales Gorge Member|33540|5|Briefly described|p886|||||||||
5139|Dales Gorge Member|33542|6|Mentioned|p412|||||||||
5139|Dales Gorge Member|33544|3|Fully described|p41|||See also pp42 - 72. Discussion of definition||||||04-AUG-15
5139|Dales Gorge Member|33545|5|Briefly described|p113|||||||||
5139|Dales Gorge Member|33687|5|Briefly described|p917|||Also P920 re mineralization||||||
5139|Dales Gorge Member|34023|4|Described|p48|||Type section Fig.9.||||||
5139|Dales Gorge Member|34203|5|Briefly described|p15|||||||||
5139|Dales Gorge Member|34541|6|Mentioned|p53|||See also PP54,56||||||
5139|Dales Gorge Member|34542|6|Mentioned|p94|||||||||
5139|Dales Gorge Member|35052|6|Mentioned|Fig.2|||||||||
5139|Dales Gorge Member|35260|4|Described|p11|||||||||
5139|Dales Gorge Member|35269|6|Mentioned|p309|||||||||
5139|Dales Gorge Member|35299|5|Briefly described|p893|||||||||
5139|Dales Gorge Member|35539|6|Mentioned|p325|||Phosphorus content of iron deposits discussed||||||
5139|Dales Gorge Member|35977|6|Mentioned|p115|||||||||
5139|Dales Gorge Member|36003|6|Mentioned|p1032|||||||||
5139|Dales Gorge Member|36004|4|Described|p1089|||Discussion re sedimentology||||||
5139|Dales Gorge Member|36091|5|Briefly described|p572|||||||||
5139|Dales Gorge Member|36247|4|Described|p188|||See also Fig.2.||||||
5139|Dales Gorge Member|36260|5|Briefly described|p78, p80|Paleoproterozoic|Paleoproterozoic|Basal unit of the Brockman Iron Formation. Geological Province: Hamersley Basin. Contains main body of iron ore of Mount Tom Price deposit.||||||07-NOV-08
5139|Dales Gorge Member|36642|6|Mentioned|Table 1|||||||||
5139|Dales Gorge Member|36882|4|Described|p129|||||||||
5139|Dales Gorge Member|37170|6|Mentioned|p198|||||||||
5139|Dales Gorge Member|37226|6|Mentioned|Fig.1|||||||||
5139|Dales Gorge Member|37297|6|Mentioned|p96|||||||||
5139|Dales Gorge Member|37460|3|Fully described|p115|||||||||
5139|Dales Gorge Member|37577|6|Mentioned|p30|||||||||
5139|Dales Gorge Member|37704|6|Mentioned|Fig.1|||||||||
5139|Dales Gorge Member|37708|6|Mentioned|p1929|||||||||
5139|Dales Gorge Member|38102|6|Mentioned|p189|||||||||
5139|Dales Gorge Member|39171|6|Mentioned|p80|||||||||
5139|Dales Gorge Member|39200|4|Described|p286|||||||||
5139|Dales Gorge Member|39558|6|Mentioned|Table 1|||||||||
5139|Dales Gorge Member|39589|6|Mentioned|p158|||||||||
5139|Dales Gorge Member|39697|6|Mentioned|p126|||||||||
5139|Dales Gorge Member|39837|6|Mentioned|p267|||||||||
5139|Dales Gorge Member|39952|5|Briefly described|p289|||||||||
5139|Dales Gorge Member|40369|6|Mentioned|p5|||||||||
5139|Dales Gorge Member|40790|6|Mentioned|p193|||||||||
5139|Dales Gorge Member|40852|5|Briefly described|p23|||||||||
5139|Dales Gorge Member|41358|5|Briefly described|p145|||||||||
5139|Dales Gorge Member|41622|6|Mentioned|p272|||||||||
5139|Dales Gorge Member|41768|6|Mentioned|p28|||||||||
5139|Dales Gorge Member|41847|6|Mentioned|p107|||||||||
5139|Dales Gorge Member|42112|5|Briefly described|p9|||||||||
5139|Dales Gorge Member|42190|6|Mentioned|p274|||||||||
5139|Dales Gorge Member|42471|4|Described|p8|||of Brockman Iron Formation||||||
5139|Dales Gorge Member|42495|5|Briefly described|p35|||||||||
5139|Dales Gorge Member|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
5139|Dales Gorge Member|42730|5|Briefly described|p12|||||||||
5139|Dales Gorge Member|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
5139|Dales Gorge Member|42744|4|Described|p5|||of Brockman Iron Formation.||||||
5139|Dales Gorge Member|42785|5|Briefly described|p262|||of Brockman Iron Formation.||||||
5139|Dales Gorge Member|43063|6|Mentioned|p49|||of Brockman Iron Formation||||||
5139|Dales Gorge Member|43119|5|Briefly described|p10|||of Brockman Iron Formation||||||
5139|Dales Gorge Member|43210|5|Briefly described|Table 1 p3,p5.||Paleoproterozoic|of Brockman Iron Formation.||||||07-NOV-08
5139|Dales Gorge Member|43262|5|Briefly described|Map Legend||Proterozoic|of Brockman Iron Formation.||||||
5139|Dales Gorge Member|43290|5|Briefly described|p6||Proterozoic|of Brockman Iron Formation. U-Pb zircon age of 2490+/-20 Ma.||||||
5139|Dales Gorge Member|43595|4|Described|Table 2-29,p219|||Deposition 2490 Ma||||||
5139|Dales Gorge Member|43644|6|Mentioned|Fig.4,p591|||||||||
5139|Dales Gorge Member|43673|6|Mentioned|p374|||Ejecta Age: approx.2.5 Ga||||||
5139|Dales Gorge Member|44152|4|Described|p164, p178-187|||Detailed type section given. Comparison of this with similar BIF units of Hamersley Group on p185. The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.|c.2490 Ma.|Basal Brockman Iron Formation.||Overlies Mount McRae Shale. Is overlain by Whaleback Shale Member.|BIF.|
5139|Dales Gorge Member|48760|6|Mentioned|p125|||||||||
5139|Dales Gorge Member|50227|5|Briefly described|p442, p443 Fig. 1|Paleoproterozoic|Paleoproterozoic|BIF-rich unit of Brockman Iron Formation. Conformably overlies both Mount McRae Shale and Mount Sylvia Shale Formation. Max. thickness: ~150m in type section near Wittenoom. Age: 2470Ma.Geol Prov:  Hamersley Province.||||||07-FEB-11
5139|Dales Gorge Member|50549|5|Briefly described|p1158|Paleoproterozoic|Archean|Contains some of the world's largest iron ore deposits. Banded Iron Formations interbedded with shale.||||||07-NOV-08
5139|Dales Gorge Member|60373|6|Mentioned|p145 Tb. 1|Archean|Archean|Of Brockman Iron Formation.||||||23-JUN-09
5139|Dales Gorge Member|60706|4|Described|p623 Fig.2, p631|Paleoproterozoic|Paleoproterozoic|Basal member of the Brockman Iron Formation. Age: 2461+/-6Ma, 2481+/-4Ma, 2454+/-18Ma, 2495+/-16Ma (SHRIMP). Geological Province: Hamersley Basin. Comprises of well-banded BIF made up of chert and iron oxides; with 3 distinct scales of banding.||||||07-NOV-08
5139|Dales Gorge Member|61268|6|Mentioned|p84|||||||||
5139|Dales Gorge Member|61560|5|Briefly described|p498 Tb. 4|||Of the Brockman Iron Formation. Displays impact spherules caused by impact ejecta. Geological Province: Hamersley Basin.||||||
5139|Dales Gorge Member|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Of the Brockman Iron Formation.  Age: ca2.50-2470Ga. Geological Province: Hamersley Basin. See also Dales Gorge Shale Member.||||||07-NOV-08
5139|Dales Gorge Member|61847|6|Mentioned|p296 Fig. 3|||Geological Province: Pilbara Craton.||||||03-JUL-06
5139|Dales Gorge Member|62129|3|Fully described|p10, p24|Archaean|Archaean|Of Brockman Iron Formation. Overlain by Whaleback Shale Member. Age: 2490+/-20Ma (U-Pb zircon). Thickness: 150m. Geological Province: Hamersley Basin. Consists of alternating sequence of 17 BIF and 16 argillite macrobands.||||||07-FEB-11
5139|Dales Gorge Member|63153|6|Mentioned|p1360, p1362 Fig.3. |||Typically displays concentric, and less commonly chevron-style, folding.||Unit in Brockman Iron Formation.||||
5139|Dales Gorge Member|64384|5|Briefly described|p35 Tb. 6, p36|||Of Brockman Iron Formation (Hamersley Group). Overlain by Whaleback Shale. Geological province: Hamersley Basin. Comprises alternating sequence of 17 BIF and 16 shale macrobands, traceable throughout the basin. Hosts iron ore. See also p39||||||07-FEB-11
5139|Dales Gorge Member|64406|5|Briefly described|p1-2|||Of the Brockman Iron Formation. Geol. Prov: Hamersley Basin. Further subdivided into a sequence of "macrobands" consisting of 33 alternations of BIF and iron-rich shales. Used as facing stone forming lift panels in Mineral House, Perth.||||||30-SEP-08
5139|Dales Gorge Member|64725|5|Briefly described|p58.|||Contains 17 bands of BIF.|c.2480 Ma (Nelson et al. 1999).|Unit in Brockman Iron-formation.||Is overlain by Whaleback Shale Member.||03-APR-12
5139|Dales Gorge Member|65683|5|Briefly described|p801 Fig2|||Of Brockman Iron Formation. Underlies Whaleback Shale Member; overlies Mount McRae Shale.||||||08-MAR-12
5139|Dales Gorge Member|65757|5|Briefly described|p81 Tb.2, p84 Fig.2, p88|Siderian|Siderian|part of the Brockman Iron Formation. Ferruginous volcanic tuffs, 2-3m thick with 10-20cm of potassium feldspar/stilpnomelare spherules. Age: 2481+/-4 Ma. Underlies the Mount Whaleback Member.||||||
5139|Dales Gorge Member|67025|5|Briefly described|p319, p328.|||Contains high-grade hematite ore; mined at Tom Price.||Basal unit in Brockman Iron Formation.||Conformably overlies Mount McRae Shale. Is overlain conformably by Whaleback Shale Member.||
5139|Dales Gorge Member|67056|4|Described|p419 Fig.2. |||Marked by lithological alternations at the metre-scale, known as macrobanding, comprising alternating magnetite-rich mesobanded BIF and non-BIF horizons. The latter consist of cherty quartz and Fe carbonates with composite volcanigenic/chemical silicate horizons. Has relatively high (~0.1 wt%) P.||Basal unit in Brockman Iron Formation.||Overlies Colonial Chert Member of Mount McRae Shale. Is overlain by Mount Whaleback Shale.|Carbonate replaced shales common.|
5139|Dales Gorge Member|67130|5|Briefly described|p3 fig 2, p8 fig 5, p9 fig 6, p42|Siderian|Neoarchean||c. 2500 Ma - 2460 Ma|Brockman Iron Formation||Overlies Mount McRae Shale, overlain by Whaleback Shale Member|Banded iron formation|
5139|Dales Gorge Member|67201|4|Described|p34, p52, 54-55|||Gently to tightly folded.|c. 2495 Ma near base, U-Pb SHRIMP|Brockman Iron Formation||Is overlain by Whaleback Shale Member.|BIF-dominated; includes distinct scales of banding. Alternating BIF and shale macrobanding reflected by stepped nature of cliffs in the gorge.|
5139|Dales Gorge Member|67721|5|Briefly described|p38 Fig.9|Siderian|Siderian|Approximately 150 m thick.|c. 2479-2473 Ma|Of the Brockman iron formation.|||Banded iron formation, divided into six zones.|
5139|Dales Gorge Member|67827|6|Mentioned|p414 Fig.4|||Wittenoom and Paraburdoo.|||||Contains BIF.|
5139|Dales Gorge Member|67855|6|Mentioned|p226|||||Of Brockman Iron Formation||||
5139|Dales Gorge Member|68035|4|Described|p292 Fig 6|Paleoproterozoic|Paleoproterozoic|Hamersley Group, Hamersley Basin.|2481 - 2461 Ma|Of Brockman Iron Formation.||Overlies Mount McRae Shale. Overlain by Whaleback Shale Member.|Banded iron formation.|
5139|Dales Gorge Member|68141|5|Briefly described|p195|Precambrian|Precambrian|Pilbara Craton. Ge/Si measurements suggest silica in BIF layers was derived from weathering of continental land masses rather than hydrothermal fluxes.|2.5 Ga.|Hamersley Group.|||Chert, BIF.|
5139|Dales Gorge Member|68280|5|Briefly described|p5, p41|Paleoproterozoic|Paleoproterozoic||c. 2495 Ma|Brockman Iron Formation||overlain by Whaleback Shale Member|Banded iron formation with alternating microbands of shale and iron at 0.3-1.7mm intervals.|
5139|Dales Gorge Member|69267|6|Mentioned|p658||||||||Shows regular alternation of fine chert and magnetite laminae.|
5139|Dales Gorge Member|69538|5|Briefly described|p516, p517 Fig.3, p524, p529 Fig.9|||See also p531 Fig.11, p537-538, p551 Fig.27, p564, p568, p571, p583-585. ||Unit in Brockman Iron Formation.||Overlies Mount McRae Shale. Is overlain by Whaleback Shale Member.||
5139|Dales Gorge Member|69563|5|Briefly described|p689-691, p696|||Contains a ~20cm microkrystite-rich (spherule) unit, overlain by BIF. Consistent with a 200-300km diameter source impact crater.|2481 +/- 4 Ma; Trendall et al. (2004).|Unit in Brockman Iron Formation.|||Abundant tuffaceous intercalations within BIF bands.|
5139|Dales Gorge Member|69745|5|Briefly described|p268, 272, 277-282, 284, 286, 288-290|Proterozoic|Proterozoic|Hamersley Province. An unmineralised section forms a prominent cliff at Mount Wall. Contains 3 submembers and distinctive 17 BIF macrobands. Hosts high-grade iron ores in a variety of mineral forms. Differences between mineralised and unmineralised occurrences detailed.||Brockman Iron Formation.|||Blue to grey banded rocks dominated by chert and magnetite with only smaller amounts of hematite, riebeckite, carbonate and other Fe-silicates.|
5139|Dales Gorge Member|70509|5|Briefly described|p14,25,29-30,32,34|Paleoproterozoic|Paleoproterozoic|Geological province: Hamersley Province; Pilbara Craton. Also referred to as Dales Gorge BIF in text. Underwent minor folding and basinal uplift; associated low-grade regional metamorphism from burial prehnite-pumpellyite facies to greenschist facies (Smith et al., 1982).||Unit of Brockman Iron Formation.||Lowermost unit of Brockman Iron Formation. Overlain by Whaleback Shale Member. Underlain by Mount McRae Shale.||
5139|Dales Gorge Member|71513|6|Mentioned|p66-69, p71, p75, p77-82, p86, p88|Precambrian|Precambrian|Widespread distribution, highly preserved and economically significant as the main host rock to giant iron-ore deposits. Intersected in drillholes DDH44 and Mitchell-2.||Brockman Iron Formation||||
5139|Dales Gorge Member|71785|2|Defined|p86-91|||Member Brockman Iron Fm.||||||
5139|Dales Gorge Member|71808|4|Described|viii, p7, p10, p19-p20, p27-p28, p30-p31|||Hamersley Province. At Witternoom Gorge the upper part of DS4 is a bolide derived Bouma sequence. Relatively monotonous lithology. The type section occurs in hole 47A (Trendall and Blockley, 1970). Bedding described in great detail.  See also p33, p40, p44, p47, p52-p53, p67, p83, p85-p86, p98, p102-p103, p106, p117, p135, p187, p193-p196, p198-p199, p230-p231, p235-p236, p244.||Brockman Iron Formation|Includes the Colonial Chert Member.|Overlain by the Mount Whaleback Shale Member.|Micro and meso-banded iron formation with turbiditic to tuffaceous S macrobands,|
5139|Dales Gorge Member|72254|6|Mentioned|p365|||||||||
5139|Dales Gorge Member|72493|4|Described|p27-37, 39-41, 43-44|Neoarchaean|Neoarchaean|Hamersley Basin. Referred to as DGM from p28. The composite type section is assembled from drillcores 47A, Y1 and EC10 in Wittenoom Gorge (22deg 20min S, 118deg 14min E). c.140m thick. A variety of ages is presented, and deposition rates discussed.|c.2495 - 2461 Ma.|Brockman Iron Formation.||Overlies Mount McRae Shale. Is overlain by Whaleback Shale Member.|A ""classic"" BIF: consists almost entirely of chert and iron oxides. Has three distinctive scales of stratification, the cause(s) of which constitute the focus of this study.|
5139|Dales Gorge Member|72569|6|Mentioned|p2, p21|||Of the Hamersley Basin.||Brockman Iron Formation||||
5139|Dales Gorge Member|72712|6|Mentioned|p10.|Siderian|Siderian|Easily recognizable despite the tight folding in the core of the Hardey Syncline.|c. 2495 Ma to c. 2460 Ma.|?Base of Brockman Iron Formation.||Possibly overlies Mount McRae Shale and Mount Sylvia Formation and probably overlain by Whaleback Shale Member.||
5139|Dales Gorge Member|72758|5|Briefly described|p15 Tb.1, p25-27.|||These units are present over much of northeastern Wyloo.||?Base of Brockman Iron Formation||Overlies Whaleback Member and underlies Weeli Wolli Formation.|Banded iron formation and shale macrobands. BIFS subdivided into chert and chert matrix mesobands.|
5139|Dales Gorge Member|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Brockman Iron Formation||Overlies the Colonial Chert Member, underlies the Whaleback Shale Mmeber|Banded iron formation with lesser shale, minor Fe-chert.|
5139|Dales Gorge Member|73290|6|Mentioned|p783-785|||||Brockman Iron Formation.|||Contains magnetite mesobands.|
5139|Dales Gorge Member|73538|5|Briefly described|p1-2, p4-8|Siderian|Siderian|An age of ca 2480 Ma was reported by Trendall et al. (2004). [Written as Dales Gorge Iron Formation on p1, 5-8 and as Dales Gorge formation on p2].|ca 2480 Ma|Brockman Iron Formation||Underlain by McRae Shale. Overlain by Whaleback Shale.|Iron formation.|
5168|Dampier Limestone|11797|5|Briefly described|map legend|Pleistocene|Pleistocene|Shark Bay Area. Undifferentiated Bibra Limestone and Dampier Limestone also shown on map.|||||Shelly calcarenite to calcirudite; shallow marine and beach-ridge deposits; extensive calcretization.|
5168|Dampier Limestone|23726|5|Briefly described|p95|Pleistocene|Pleistocene|Overlain by Bibra Limestone. Geological Province: Carnarvon Basin.||||||13-OCT-08
5168|Dampier Limestone|23768|6|Mentioned|p134-135|Late Pleistocene|Late Pleistocene|See also Dampier Formation.||||||
5168|Dampier Limestone|38485|4|Described|p19|||Formerly Dampier Formation||||||
5168|Dampier Limestone|38998|4|Described|p17|||||||||
5168|Dampier Limestone|40340|6|Mentioned|Table 2|||||||||
5168|Dampier Limestone|40342|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
5168|Dampier Limestone|40343|5|Briefly described|p13|||||||||
5168|Dampier Limestone|40617|6|Mentioned|p18|||||||||
5168|Dampier Limestone|41271|4|Described|p197|||||||||
5168|Dampier Limestone|41438|6|Mentioned|Fig.23|||||||||
5168|Dampier Limestone|42116|5|Briefly described|Fig.1 P6|||||||||
5168|Dampier Limestone|67200|5|Briefly described|p8 fig 6, |Quaternary|Pliocene|||||Overlies Peron Sandstone, overlain by Bibra Limestone|Parallel bedded limestone with invertebrate macrofossils.|
5168|Dampier Limestone|69558|4|Described|p24, p98, p99, p100, p191 fig 296|Pleistocene|Pleistocene|Originally the Dampier Formation of Logan et al. (1970b) Renamed the Dampier Limestone by Van de Graaff et al (1983). May be partly equivalent to the Depuch and Bibra Limestones. Deposited during the last interglacial period of the Pleistocene. 21 bivalve and nine gastropod species have been identified in a quarry southeast of the old Flint Cliff Telegraph Station. Forms substrate on which the Shark Bay stromatolites grow. See also p192 fig 298, p226.|||Includes the Carbla Oolite Member.||Shelly and coralline limestone and sandstone.|
5175|Dandar Sandstone|32648|6|Mentioned|p32|||Cret.||||||
5177|Dandaragan Sandstone|23279|6|Mentioned|p30|||(Cockbain and Playford, 1973).||||||
5177|Dandaragan Sandstone|23816|4|Described|p246, 248|Early Cretaceous|Early Cretaceous|Formerly known as the "Dandaragan Series". Geological Province: Perth Basin. Of the Warnbro Group. Underlying unit: Yarragadee Formation. Overlying unit: Molecap Greensand (conformable). Max. thicxkness: 33 m.||||||27-APR-05
5177|Dandaragan Sandstone|24094|5|Briefly described|p268|Cretaceous|Cretaceous|Overlain by Gingin Chalk formation (disconformably). Geological Province: Perth Basin.||||||16-MAR-05
5177|Dandaragan Sandstone|24160|6|Mentioned|p95 Tb.57.|||||||Unconformably overlies Leederville Formation.||
5177|Dandaragan Sandstone|24351|5|Briefly described|Plate 3 (in pocket)|Certaceous|Cretaceous|Log Houtman-1.||||||13-DEC-07
5177|Dandaragan Sandstone|29693|6|Mentioned|p66|||||||||
5177|Dandaragan Sandstone|30188|2|Defined|p74|Early Cretaceous|Early Cretaceous|||||||
5177|Dandaragan Sandstone|31153|6|Mentioned|Fig. 57|||Table refers Cockbain & Playford (1973)||||||
5177|Dandaragan Sandstone|31238|4|Described|p27|||||||||
5177|Dandaragan Sandstone|31562|6|Mentioned|Fig. 3|||||||||
5177|Dandaragan Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
5177|Dandaragan Sandstone|33627|6|Mentioned|p582|||||||||
5177|Dandaragan Sandstone|35282|6|Mentioned|Fig.2|||||||||
5177|Dandaragan Sandstone|35638|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5177|Dandaragan Sandstone|35968|5|Briefly described|p64|||See also Fig.8.||||||
5177|Dandaragan Sandstone|36257|6|Mentioned|Table 2.1|||||||||
5177|Dandaragan Sandstone|36293|2|Defined|p172|Aptian|Aptian|||||||
5177|Dandaragan Sandstone|36890|3|Fully described|p248|||Formerly Dandaragan Series||||||
5177|Dandaragan Sandstone|37341|6|Mentioned|p230|||||||||
5177|Dandaragan Sandstone|40348|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
5177|Dandaragan Sandstone|40349|5|Briefly described|p16|||||||||
5177|Dandaragan Sandstone|41989|4|Described|p113|||||||||
5177|Dandaragan Sandstone|42123|6|Mentioned|Table 1 P3|||||||||
5177|Dandaragan Sandstone|42995|5|Briefly described|Table 1|||||||||
5177|Dandaragan Sandstone|43564|6|Mentioned|p462|||||||||
5177|Dandaragan Sandstone|44144|4|Described|p504 Tb.4-21, p517|Aptian|Barremian|Type Section: West of Dandaragan 30o41'30''S 115o38'30''E. 31m thick shallow marine deposits.||Warnbro Group||Overlies Parmelia Formation unconformably. Overlain by Molecap Greensand disconformably. Partial correlation with upper parts of Leederville Formation.|Medium- to coarse-grained feldspathic sandstone, grading to fine conglomerate.|
5177|Dandaragan Sandstone|61811|5|Briefly described|p57.|||Type section details in Appendix 1. Name has fallen into disuse.||Unit in Warnbro Group.||Is overlain by Poison Hill Greensand.||
5177|Dandaragan Sandstone|64580|6|Mentioned|map legend|||Of Warnbro Group.||||||
5177|Dandaragan Sandstone|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p55, Ch2 p57|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Coolyena Group||Unconformably overlies the Leederville Formation. Overlain by the Osborne Formation.||
5177|Dandaragan Sandstone|70097|5|Briefly described|p20 Fig.4|Albian|Aptian|Northern Perth Basin. Dandaragan Trough.||Coolyena Group||Overlies South Perth Shale (Warnbro Group). Is overlain by Osborne Formation.|Sandstone.|12-SEP-17
5177|Dandaragan Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
5253|Darwin Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p222|Early Cretaceous|Early Cretaceous|Name of Hughes (1978) and Mory (1988). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Also on p228 Fig. 18 and p230.||||||01-MAR-10
5253|Darwin Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Aptian|Valanginian|Up to 52m thick. Type section: Cliffs at Fanny bay, Darwin. 12o27'S 130o50'E.  Overlain by Wangarlu Formation (conformably).||Bathurst Island Group||Overlies Flamingo Group, Sahul Group (both disconformably).|Claystone, radiolarian shale and radiolarite overlying glauconitic sandstone and shale with minor conglomerate.|
5253|Darwin Formation|13267|6|Mentioned|p278.|Early Cretaceous|Early Cretaceous|||||Overlies Echuca Shoals Formation. Is overlain by Jamieson Formation.|Radiolarite.|
5253|Darwin Formation|22663|6|Mentioned|NT97 -1-4 p3|||||||||
5253|Darwin Formation|23376|4|Described|p229 Fig.2; p227, 244-5||Aptian|Of Bonaparte Basin.||||||08-AUG-06
5253|Darwin Formation|23999|3|Fully described|p9|Early Cretaceous|Early Cretaceous|Basal unit of Bathurst Island Gp. Unconformably overlies a Proterozoic basement - Burrell Creek Fm, Koolpinhay Dolomite and Woldman Siltst; conformably overlain by Wangarlu Fm. Thick: 63m. Geol Prov: Money Shoal Basin.||||||26-APR-13
5253|Darwin Formation|24001|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Claystone, radiolaria-rich, glauconitic sandstone, bioturbated beds, silicified claystone, clayey sand, basal conglomerate,||||||
5253|Darwin Formation|24047|5|Briefly described|p13|Cretaceous|Cretaceous|||||||
5253|Darwin Formation|24085|4|Described|p33|Early Cretaceous|Early Cretaceous|Of Bathurst Island Group. Marine-reptile bearing deposits.||||||20-JUL-06
5253|Darwin Formation|24122|5|Briefly described|p14|Cretaceous|Cretaceous|Of Bathurst Island Group.  Overlies the Petrel Formation.||||||
5253|Darwin Formation|24234|5|Briefly described|p287 Fig.3|Aptian|Aptian|Overlain by Jamieson Formation. Geological Province: Bonaparte Basin.||||||
5253|Darwin Formation|24297|5|Briefly described|p21|Cretaceous|Cretaceous|Of Bathurst Island Group.||||||
5253|Darwin Formation|24442|6|Mentioned|p2|||Includes the "Howard Sand Member".||||||
5253|Darwin Formation|24569|5|Briefly described|p248 Fig. 3|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
5253|Darwin Formation|39069|6|Mentioned|p1|||||||||
5253|Darwin Formation|41459|6|Mentioned|Fig.2|||||||||
5253|Darwin Formation|41532|3|Fully described|p306|||||||||
5253|Darwin Formation|41731|6|Mentioned|Fig.3|||||||||
5253|Darwin Formation|42003|6|Mentioned|p111|||||||||
5253|Darwin Formation|42056|4|Described|p98|||||||||
5253|Darwin Formation|42442|2|Defined|p27|Aptian|Valanginian|||||||
5253|Darwin Formation|43661|6|Mentioned|Fig.3|||||||||
5253|Darwin Formation|43699|6|Mentioned|Fig.6,p10||Early Cretaceous|||||||
5253|Darwin Formation|43739|6|Mentioned|Fig.5,p38||Early Cretaceous|||||||
5253|Darwin Formation|43829|5|Briefly described|Fig.2,p225|Aptian|Valanginian|||||||
5253|Darwin Formation|44235|14|Not recorded|p.117||Early Cretaceous|L. Cretaceous.||||||
5253|Darwin Formation|44965|14|Not recorded|Not recorded|||||||||
5253|Darwin Formation|45011|14|Not recorded|No page listed||Albian|See also Lexicon. Regarded as part of Mullaman Group.||||||
5253|Darwin Formation|45022|14|Not recorded|p.108||Late Cretaceous|||||||
5253|Darwin Formation|45121|6|Mentioned|p45|||Refers Noakes(1949)||||||
5253|Darwin Formation|49637|5|Briefly described|Fig. 3|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Geological Province: Darwin Shelf.||||||07-FEB-11
5253|Darwin Formation|60386|6|Mentioned|p302|Valanginian|Berriasian|Bonaparte Basin. Distal shelf/basin. ||||||
5253|Darwin Formation|60677|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Clayey sand, sandy clay, ferruginised at surface. Of Bathurst Island Group.||||||
5253|Darwin Formation|60685|5|Briefly described|p20|Mesozoic|Mesozoic|Of the Bathurst Group. Shallow marine mudstone dominated unit. Along with the Petrel Formation, equivalent to the former "Mullaman Beds".||||||
5253|Darwin Formation|61548|6|Mentioned|p480 Fig.3|Aptian|Aptian|Northern Bonaparte Basin.||||||
5253|Darwin Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Neocomian|Of the Bathurst Island Group. Age: ~135-~104Ma. Geological Province: Northern Bonaparte Basin, Petrel Sub-basin and Money Shoals Basin.||||||01-MAR-10
5253|Darwin Formation|63062|5|Briefly described|p9 Fig. 9|Early Cretaceous|Early Cretaceous|Included in terms of equivalents. Geological Province: Arafura and Money Shoal Basins.||||||07-FEB-11
5253|Darwin Formation|64769|6|Mentioned|p9|Cretaceous|Cretaceous|||||||
5253|Darwin Formation|65339|5|Briefly described|p6 Table 1, p16.|||Average thickness c.30 m.||Basal unit in Bathurst Island Group.||Unconformably overlies Koolpinyah Dolostone.|Sandstone and claystone, some of which is currently unconsolidated.|
5253|Darwin Formation|67564|6|Mentioned|p51.|Cretaceous|Cretaceous|Partly correlated with the now defunct Mullaman beds.||||||
5253|Darwin Formation|68223|6|Mentioned|p178 Fig.3|Aptian|Aptian|||||||
5253|Darwin Formation|69297|6|Mentioned|p290|Cretaceous|Cretaceous|Money Shoal Basin. ||||||
5253|Darwin Formation|69420|5|Briefly described|p5:117|Cretaceous|Cretaceous|The lowermost part of this unit has been altered into a silicified mottled claystone known as porcellanite, used as a building stone in Darwin and still intermittently quarried.||Bathurst Island Group.|Howard Sand Member.|||12-JUL-16
5253|Darwin Formation|69452|4|Described|p36:8, 15, 22|Albian|Aptian|Money Shoal Basin; also Petrel Sub-basin, Bonaparte Basin, where the rocks are referred to as Darwin Formation equivalent. Referred to as Darwin Radiolarite by Geoscience Australia (2009, 2011). Onshore and offshore. Formerly included the basal Valanginian-Aptian interval of glauconitic shale; this has been renamed the Echuca Shoals Formation. <52m thick. Shallow marine deposits.||Bathurst Island Group.||Overlies Echuca Shoals Formation (offshore) conformably, and ?Kinmore Group (onshore) unconformably. Is overlain conformably by Wangarlu Formation.|Radiolarian chert, claystone and calcimudstone.|12-JUL-16
5253|Darwin Formation|69455|5|Briefly described|p39:5|||Regionally extensive: Money Shoal Basin and Petrel Sub-basin of the Bonaparte Basin in the Joseph Bonaparte Gulf.||||Overlies Plover Formation.|Dominated by shallow-marine mudstones.|12-JUL-16
5253|Darwin Formation|69456|3|Fully described|p40:2; 40:3 Fig.40.4; 40:4-8, 13-14|Early Cretaceous|Early Cretaceous|Hughes (1978); Mory (1988). Originally the "Port Darwin Beds" of Jensen (1914). Subsequently the upper part of the Mullaman Group (Noakes, 1949), later the Mullaman Beds (Skwarko, 1966). The equivalent unit in the offshore Bonaparte Basin has been named the Darwin Radiolarite (Geoscience Australia, 2011). Unconformably overlies Proterozoic rocks of the Pine Creek Orogen. Southern Money Shoal Basin, eastern Bonaparte Basin. Is exposed in the Darwin region; has been intersected in drillholes in Bathurst and Melville Islands, the Cobourg Peninsula, and in the offshore area. Shallow-marine, neritic environment. Up to 63m thick. Aptian age. Capped by a lateritic duricrust in the Darwin area. Source of porcellanite (local term for silicified mottled claystone) used for building and ornamental landscape stone. Equivalent to the Darwin Radiolarite. Contains marine fossils and microplankton.||Basal Bathurst Island Group.|Howard Sand member.|Unconformably overlies Burrell Creek Formation, Wildman Siltstone and Koolpinyah Dolostone. Is overlain conformably by Wangarlu Formation. Lateral equivalent to Marligur Formation.|Claystone and minor silty claystone, sandy claystone, phosphatic nodular claystone; radiolarian siltstone; partially lithified clayey sandstone; clean sandstone and glauconitic sandstone; locally developed basal conglomerate.|12-JUL-16
5253|Darwin Formation|69653|5|Briefly described|p6, 8, 10, 26-27, 38, 41-43, 50-51, 53|Cretaceous|Cretaceous|Petrel Sub-basin. Shoreface-offshore deposits. Schematic (gamma ray) well sections. Composite well diagram. See also p61, 63.||Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Wangarlu Formation.|Glauconitic siltstone interbedded with mudstone, glauconitic mudstone. Facies described in detail.|
5253|Darwin Formation|69673|6|Mentioned|p204|Cretaceous|Cretaceous|20-63m thick.||Bathurst Island Group||Equivalent to Marligur Formation||
5253|Darwin Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Aptian|Aptian|See also Regional geology: Fig.6, p10, p14. Sahul: Fig.2, p1-2. , where shown as Aptian - Albian. Has oil shows which likely originated from the Echuca Shoals Formation. Reservoir carbonates in Sahul Syncline.||Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Wangarlu Formation.||23-SEP-18
5253|Darwin Formation|70098|5|Briefly described|p19 Fig.5|Early Cretaceous|Early Cretaceous|||Flamingo Group||Is overlain by Bathurst Island Group (and equivalent?).||
5253|Darwin Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, shale|
5276|Davis Dolerite|23594|5|Briefly described|p20|||Geological Province: Bangemall Basin.||||||
5276|Davis Dolerite|24025|5|Briefly described|p15|||Intrudes the Woblegun Formation of the Manganese Group. Geological Province: Collier Basin.||||||17-JUL-08
5276|Davis Dolerite|24110|5|Briefly described|Plate 1|Proterozoic|Proterozoic|Geological Province: Collier Basin.||||||22-APR-09
5276|Davis Dolerite|24183|5|Briefly described|p6|Stenian|Stenian|Of the Manganese Group. Age: ~1050 Ma.||||||
5276|Davis Dolerite|34135|6|Mentioned|p16|||Middle Proterozoic||||||
5276|Davis Dolerite|36551|6|Mentioned|p90|||||||||
5276|Davis Dolerite|37707|6|Mentioned|p25|||||||||
5276|Davis Dolerite|39426|6|Mentioned|p13|||||||||
5276|Davis Dolerite|39697|5|Briefly described|p132|||||||||
5276|Davis Dolerite|40089|6|Mentioned|Plate 1|||||||||
5276|Davis Dolerite|41669|3|Fully described|p43|||||||||04-FEB-10
5276|Davis Dolerite|41768|6|Mentioned|p46|||||||||
5276|Davis Dolerite|42708|5|Briefly described|Plate 1|Proterozoic||||||||
5276|Davis Dolerite|43055|5|Briefly described|p26|||||||||
5276|Davis Dolerite|43056|5|Briefly described|Map Legend|||||||||14-NOV-08
5276|Davis Dolerite|44297|4|Described|p.5,7-20|||(F51-9).||||||04-FEB-10
5276|Davis Dolerite|44298|5|Briefly described|map legend||Proterozoic|||||||04-FEB-10
5276|Davis Dolerite|44831|5|Briefly described|Map Legend||Proterozoic|||||||
5276|Davis Dolerite|50188|6|Mentioned|p17|||Intrudes Manganese Group on BALFOUR DOWNS.||||||16-JUL-08
5276|Davis Dolerite|63417|5|Briefly described|Map legend|Cambrian|Cambrian|Age: c. 523Ma. Intrudes the undivided portion of Manganese Group (Bangemall Supergroup).  Geological Province: Collier Basin. Fine- to medium-grained dolerite; in sills, contains magnetite.||||||23-JUL-07
5276|Davis Dolerite|64384|6|Mentioned|p92|||Sills and associated dykes. With mineralogy similar to that of the Murraminda Dolerite.||||||07-FEB-11
5276|Davis Dolerite|67183|4|Described|p639,643,645,647,649,655,661-2,665-72|Mesoproterozoic|Mesoproterozoic|Intrusion related to the D2b extensional event. Present in the south-western Oakover Basin. Most likely part of the ca 1070 Ma Bangemall Supergroup of the Warakurna Large Igneous Province. ca 1050 Ma K-Ar age for dolerite sill of the Manganese Subgroup. |ca 1090-1050 Ma, |Manganese Subgroup||Intrudes shales of the Balfour Formation.|Dolerite dykes and sills.|
5276|Davis Dolerite|67202|5|Briefly described|p52|Cambrian|Cambrian||c.523 Ma (Hickman, 1978).|||Intrudes Woblegun Formation.||
5276|Davis Dolerite|69003|6|Mentioned|p4|||Capricorn Orogen.||||||
5276|Davis Dolerite|69167|4|Described|geologyp_lut.csv|Cambrian|Cambrian||||||Dolerite in sills and dykes; fine to medium grained.|
5276|Davis Dolerite|69590|4|Described|GEOL_LUT_CSV files|Cambrian|Cambrian|Of Kalkarindji Large Igneous Province. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|523 Ma (isotopic)||||Dolerite in sills and dykes; fine to medium grained|
5276|Davis Dolerite|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|||||||
5276|Davis Dolerite|71042|5|Briefly described|p64 fig 1, p66 fig 2, p68|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province, Oakover Basin. Age from glauconite in the Coondoon Formation and is interpreted here as a minimum age for the intrusion of this unit. See also  p68-p71, p80, p82.|1050 Ma (K-Ar, Goode and Hall, 1981)|||Intrudes the Balfour Formation.||24-MAY-19
5276|Davis Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
5276|Davis Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Cambrian||523+/-14 Ma.||||Dolerite in sills and dykes; fine to medium grained.|
5296|DeGrey River Alluvium|35711|6|Mentioned|Fig.11|||||||||
5300|Dean Quartzite|22506|6|Mentioned|p130 Fig.4|Cryogenian|Tonian|||||||
5300|Dean Quartzite|22561|6|Mentioned|p15|||||||||
5300|Dean Quartzite|22562|5|Briefly described|p33|||Equivalent to Heavitree Quartzite.||||||08-AUG-06
5300|Dean Quartzite|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
5300|Dean Quartzite|22803|5|Briefly described|p423|||||||||
5300|Dean Quartzite|22804|5|Briefly described|p441|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|22805|5|Briefly described|p464|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|22826|5|Briefly described|p568|Neoproterozoic|Neoproterozoic|||||||
5300|Dean Quartzite|23716|6|Mentioned|p4|||Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|24301|4|Described|p14, p7 Tb. 2,|Neoproterozoic|Neoproterozoic|Undated but is suggested to be equivalent to the Neoproterozoic Heavitree Quartzite. Overlain by Pinyinna beds.  Geological Province: Amadeus Basin.||||||16-JUN-09
5300|Dean Quartzite|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Medium- to coarse-grained, thick-bedded to massive white quartzite and quartz sandstone; minor conglomerate and fine-grained sheared quartzite. Geological Province: Amadeus Basin.||||||16-JUN-09
5300|Dean Quartzite|24496|5|Briefly described|p21 Tb.2|Neoproterozoic|Neoproterozoic| Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|30389|6|Mentioned|Table 1|||Mid Proterozoic age. Lithology.||||||
5300|Dean Quartzite|30390|5|Briefly described|p32|||||||||
5300|Dean Quartzite|30602|6|Mentioned|p658|||||||||
5300|Dean Quartzite|30670|6|Mentioned|p67|||Upper Proterozoic age||||||
5300|Dean Quartzite|30815|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5300|Dean Quartzite|30817|4|Described|p9|||See also p14. Correlated with Heavitree Quartzite.||||||08-AUG-06
5300|Dean Quartzite|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5300|Dean Quartzite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5300|Dean Quartzite|31991|6|Mentioned|p298|||Correlation with Heavitree Quartzite.||||||
5300|Dean Quartzite|33307|6|Mentioned|Fig.6|||||||||
5300|Dean Quartzite|33468|6|Mentioned|p214|||||||||
5300|Dean Quartzite|33588|6|Mentioned|p6|||||||||
5300|Dean Quartzite|34945|6|Mentioned|p356|||||||||
5300|Dean Quartzite|35038|6|Mentioned|p368|||||||||
5300|Dean Quartzite|35102|6|Mentioned|p1|||||||||
5300|Dean Quartzite|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5300|Dean Quartzite|36526|6|Mentioned|p154|||||||||
5300|Dean Quartzite|36886|6|Mentioned|p196|||||||||
5300|Dean Quartzite|36887|5|Briefly described|p208|||||||||
5300|Dean Quartzite|37460|6|Mentioned|p175|||||||||
5300|Dean Quartzite|37707|6|Mentioned|p24|||||||||
5300|Dean Quartzite|38157|6|Mentioned|Table VI|||||||||
5300|Dean Quartzite|39210|5|Briefly described|p40|||||||||
5300|Dean Quartzite|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
5300|Dean Quartzite|39565|6|Mentioned|p31|||||||||
5300|Dean Quartzite|40740|6|Mentioned|p1|||||||||
5300|Dean Quartzite|41190|6|Mentioned|Fig.4|||||||||
5300|Dean Quartzite|41270|6|Mentioned|Table 1|||||||||
5300|Dean Quartzite|41717|6|Mentioned|Fig.2|||||||||
5300|Dean Quartzite|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
5300|Dean Quartzite|41852|6|Mentioned|Table 1|||||||||
5300|Dean Quartzite|41884|6|Mentioned|p70|||||||||
5300|Dean Quartzite|42059|6|Mentioned|p130|||||||||
5300|Dean Quartzite|42082|6|Mentioned|Fig.3 P323|||||||||
5300|Dean Quartzite|42504|5|Briefly described|p67|||||||||
5300|Dean Quartzite|42643|6|Mentioned|p20|||Amadeus Basin||||||
5300|Dean Quartzite|42794|6|Mentioned|p9|||||||||
5300|Dean Quartzite|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Quartzite. sandstone, conglomerate, metaquartzite, kyanite schist.  Geological province: Amadeus Basin.||||||23-JAN-08
5300|Dean Quartzite|43035|4|Described|p17|||||||||
5300|Dean Quartzite|43442|6|Mentioned|p14||Neoproterozoic|C.820 Ma (Korsh & Kennard,1991)||||||
5300|Dean Quartzite|43503|6|Mentioned|50||Proterozoic|||||||
5300|Dean Quartzite|43697|6|Mentioned|p28|||||||||
5300|Dean Quartzite|44109|5|Briefly described|p164|||Together with the Townsend Quartzite, unconformably overlies the Musgrave Block units, forming the basal units of of southwestern Amadeus Basin and Northern Officer Basin.  ||||||
5300|Dean Quartzite|44139|5|Briefly described|p286, 285 Fig. 3-69|||Occurs north of Woodroffe Thrust. Correlated with Heavitree Quartzite by Wells & others (1970). Unconformably overlies Olia Gneiss and Mount Harris Volcanics. Thick sequence of quartzite and conglomerate; deformed and schistose, and metamorphosed to greenschist or amphibolite facies.| | ||||05-MAR-18
5300|Dean Quartzite|44342|6|Mentioned|p.9|||SG/53-5.||||||
5300|Dean Quartzite|44439|2|Defined|p.4,6-8,Tb.1, map||Neoproterozoic|Upper Proterozoic. (G52-2).||||||
5300|Dean Quartzite|44440|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|44493|4|Described|p.9-12,14, map||Neoproterozoic|U.Prot.Bloods Range sheet. (G53-3).||||||22-DEC-09
5300|Dean Quartzite|44494|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|44495|4|Described|p.5, map||Neoproterozoic|U.Prot.Ayers Rock sheet. (G52-8). See p.7,9, for details.||||||
5300|Dean Quartzite|44496|5|Briefly described|map legend||Neoproterozoic|Schistose quartzite, Upper Proterozoic.||||||17-JUL-06
5300|Dean Quartzite|44499|14|Not recorded|opp.p.6, Tb.1|||||||||
5300|Dean Quartzite|45041|4|Described|p20|||Proterozoic||||||
5300|Dean Quartzite|45149|6|Mentioned|Table 1|||Page 19.||||||
5300|Dean Quartzite|45170|6|Mentioned|p9|||||||||
5300|Dean Quartzite|48842|2|Defined|p.13||Neoproterozoic|p.1,5,8,10-13,26-7,30,32,Pls.3,7. Tb.I. Correlates with Heavitree Quartzite. U.Proterozic.||||||10-JUL-13
5300|Dean Quartzite|48863|14|Not recorded|p.13||Neoproterozoic|Upper Proterozoic.||||||
5300|Dean Quartzite|48864|2|Defined|p.23||Neoproterozoic|Tb.1. On many pages. p.1,9,10,12,14,15-17,20,25,30,33,36-39,41-45,47,49,50,52,Pl.4,5,6,7,8,10,11,12,13. U.Prot. (G52-2,3,7,8).||||||
5300|Dean Quartzite|48865|14|Not recorded|Pl.9|||Prelim.map Ayers Rock 1:250,000 (G52-8).||||||
5300|Dean Quartzite|48963|6|Mentioned|Fig.3|||||||||
5300|Dean Quartzite|49833|6|Mentioned|p8|||||||||
5300|Dean Quartzite|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies: Mount Harris Basalt.  Underlies: Pinyinna beds.||||||22-DEC-09
5300|Dean Quartzite|50321|5|Briefly described|Map Legned|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Underlies: Pinyinna beds.  .||||||09-JUN-04
5300|Dean Quartzite|60572|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Crystalline quartz sandstone, rare quartz conglomerate and quartz-muscovite-kyanite layers.  Geological Province: Amadeus Basin.||||||23-DEC-09
5300|Dean Quartzite|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Deformed basal sediments of Amadeus Basin.||||||22-FEB-05
5300|Dean Quartzite|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Crystalline quartz sandstone, rare vein quartz pebble conglomerate, quartz-kyanite-muscovite layers, red/purple crystalline quartz sandstone, feldspathic sandstone. Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz Sandstone. Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|60683|4|Described|p24-25, p9 Tb. 1, p22, p23|Neoproterozoic|Neoproterozoic|Recrystallised, thick-bedded to massive quartz sandstone; rare quartz conglomerate and quartz-kyanite-muscovite layers. Conformably overlain by Pinyinna beds, Bloods Range beds.  Age: probably c.850Ma. max. thickness: ~100m.  Geol. Prov: Amadeus Basin.||||||20-APR-05
5300|Dean Quartzite|61154|4|Described|p17-18, p5 Tb. 1|Neoproterozoic|Neoproterozoic|Age: ~850Ma. Max. thickness: ~60m. Overlain by/interleaved with Pinyinna beds; unconformably overlies Tjauwata Gp and Pitjantjatjara Supersuite. Geol. Prov: Amadeus Basin. See also p42 App.||||||19-JUL-05
5300|Dean Quartzite|61306|5|Briefly described|p32, p61|Proterozoic|Proterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|White crystalline quartz sandstone, quartz muscovite schist. Geological Province: Amadeus Basin.||||||23-DEC-09
5300|Dean Quartzite|61733|6|Mentioned|p47 Fig.3 |||Amadeus Basin.||||||
5300|Dean Quartzite|62359|5|Briefly described|p547-548, p550|Middle Neoproterozoic|Middle Neoproterozoic|Overlain by Pinyinna Beds. Age: ~750Ma. Geological Province: Amadeus Basin. Equivalent to Heavitree Quartzite. ||||||
5300|Dean Quartzite|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
5300|Dean Quartzite|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
5300|Dean Quartzite|62453|6|Mentioned|p16|||Age: 850Ma. Overlies Kukial Sandstone.||||||
5300|Dean Quartzite|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzite, sandstone, conglomerate. Metamorphosed in part to Kyanite schist and quartzite. Underlies Pinyinna Beds and Bitter Springs Formation.||||||14-AUG-06
5300|Dean Quartzite|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzite, sandstone, conglomerate. Metamorphosed in part to kyanite schist and quartzite.||||||
5300|Dean Quartzite|62989|5|Briefly described|p39, p40|||Unconformably overlies basement of the Musgrave Province, and Kulail Quartzite (basal unit of Amadeus Basin). Equivalent of Heavitree Quartzite. Geological Province: Amnadeus Basin. Shallow marine deposits.||||||25-JAN-07
5300|Dean Quartzite|63866|5|Briefly described|p202|||Musgrave Province.||Bentley Supergroup||||
5300|Dean Quartzite|64580|4|Described|map legend||Neoproterozoic|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally.||||||09-DEC-08
5300|Dean Quartzite|64809|5|Briefly described|p1, p3 Fig.2|Proterozoic|Proterozoic||||||Transgressive marine sands.|
5300|Dean Quartzite|65102|6|Mentioned|p363, Figure 4-38, p365, 372|Neoproterozoic|Neoproterozoic|Amadeus Basin. Correlated with Robert Formation, Townsend Formation, Pindyin beds all Officer Basin.||||||
5300|Dean Quartzite|65233|5|Briefly described|p2, p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
5300|Dean Quartzite|65256|4|Described|p17, p4, p6 Tb.1, p8, p16, p21, p37|Cryogenian|Tonian|Basal Amadeus Basin. Conformably overlies (grades into or interfingers with) Kulail Sandstone; disconformably overlies Tjauwata Group; unconformably overlies Bloods Range Formation, Pottoyu Granite Suite, Imbumbunna Granite; conformably underlies Pinyinna beds; correlative of Heavitree Quartzite; onlapped by Larapinta Group. Recrystallised, well sorted, equigranular, massive to thickly bedded quartz sandstone, rare quartz conglomerate. Probably >50m thick; strongly deformed in areas. 850 Ma (poorly constrained).||||||25-MAR-15
5300|Dean Quartzite|67128|6|Mentioned|p30|||Southern Amadeus Basin.||||||
5300|Dean Quartzite|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Unconformably overlies Arunta Complex. Is overlain by Pinyinna beds and Bitter Springs Formation.||
5300|Dean Quartzite|67553|6|Mentioned|p71|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
5300|Dean Quartzite|67856|4|Described|p342, p338, 335, 337, 344, 348|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970 etc. Base of Amadeus Basin. Type section not defined. 1200m thick. Age inferred from stratigraphic position. Mostly fluvial grading upwards to marine shelf?||||Laterally equivalent to Heavitree quartzite. Overlies Wingelina Complex (unconformably).|Fine to coarse grained quartzite; sandstone; minor conglomerate; partly metamorphosed.|
5300|Dean Quartzite|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
5300|Dean Quartzite|68270|4|Described|p683|Tonian|Tonian|Amadeus Basin.||||Overlain by Pinyinna beds. Underlain by basement.||03-JUL-19
5300|Dean Quartzite|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
5300|Dean Quartzite|68733|6|Mentioned|p190|||Amadeus Basin.|||||Texturally mature sandstone; fluvial to shallow-marine.|05-DEC-17
5300|Dean Quartzite|68996|6|Mentioned|p6|Neoproterozoic|Mesoproterozoic|Deposition ~1040-800 Ma?||||||
5300|Dean Quartzite|69003|6|Mentioned|p60-61|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
5300|Dean Quartzite|69031|5|Briefly described|p4, p6 Fig.4, p8|||Basal unit in the southern Amadeus Basin.||||Locally overlies Kulail Sandstone. Is overlain by Bitter Springs Formation. Equivalent to Heavitree Quartzite.|A lithic and feldspathic unit.|
5300|Dean Quartzite|69091|6|Mentioned|p134 Fig.6.2|||||||||26-SEP-14
5300|Dean Quartzite|69153|6|Mentioned|500k_geologyp08_lut.csv||Neoproterozoic|Lithology description shared with Heavitree Quartzite|||||Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
5300|Dean Quartzite|69436|5|Briefly described|p21:4, 9, 11, 17-19|Neoproterozoic|Neoproterozoic|Olia Chain, Amadeus Basin. Involved in thin- and thick-skinned deformation by the Petermann Orogeny, with a metamorphic assemblage of kyanite-muscovite-quartz +/- tourmaline, with rare staurolite. Is structurally interleaved with Tjauwata Group in the Wankari Detachment Zone of the Petermann Nappe Complex. Two K-Ar muscovite (metamorphism) ages of 586 +/- 5 Ma and 568 +/- 5 Ma (Close et al., 2003) have been obtained from within the Piltardi Detachment Zone.||||Overlies Amputjuta Dacite and Hull Suite. Is locally overlain (thrust fault contact) by Mount Harris Basalt and interleaved with Pinyinna beds.||12-JUL-16
5300|Dean Quartzite|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 1.||||Is overlain by Pinyinna beds. Correlated with Heavitree Quartzite.||12-JUL-16
5300|Dean Quartzite|69438|4|Described|p23:2-5, 8-10, 18, 44, 59-60|Cryogenian|Cryogenian|Extensively exposed in the SW margin of the Amadeus Basin. Shallow-marine deposits. 100-300m thick. Metamorphosed to amphibolite-grade facies, decreasing to greenschist facies to the N. Maximum deposition age from detrital zircons; minimum age from a U-Pb baddeleyite age (Glikson et al., 1996) of a spilite with affinities to those in the overlying Bitter Springs Formation. Has promising Neoproterozoic hydrocarbon reservoirs, sealed by Gillen Member salt.|Between 1050-1000 Ma and c.820 Ma. |||Conformably (gradationally) overlies Kulail Sandstone. Correlated with Heavitree Quartzite. Is overlain conformably (gradationally) by Pinyinna beds.|Widespread, sheet-like, uniform deposits of quartz sandstone; local intense silicification where the unit is exposed.|12-JUL-16
5300|Dean Quartzite|69439|6|Mentioned|p24:2|||Amadeus Basin.||||Correlative of Heavitree and Vaughan Springs Quartzites.||12-JUL-16
5300|Dean Quartzite|69440|6|Mentioned|p25:2|||Amadeus Basin. Inferred to correlate with Munyu Sandstone (Murraba Basin).||||||12-JUL-16
5300|Dean Quartzite|69606|5|Briefly described|p2, p4 fig 2, p19|Cryogenian|Cryogenian|Southern Amadeus Basin. Potential reservoir rocks.||||Overlies the Kulail Sandstone. Overlain by the Gillen Member, Bitter Springs Formation. Is equivalent to the Heavitree Quartzite.|Sandstone and quartzite.|
5300|Dean Quartzite|69673|4|Described|p63, p84, p85, p88, p89, p101|||||||Correlated with Heavitree Quartzite, overlies Kulail Sandstone, overlain by Pinyinna beds, Gillen Member|Fine to coarse grained orthoquartzite, arkosic quartzite with minor shale and conglomerate.|
5300|Dean Quartzite|69926|6|Mentioned|p156, 176, 178|||Basal quartzite in the southern Amadeus Basin. Overlies the Mulga Park Subdomain of the Musgrave Block.||||Correlated with Heavitree Quartzite.|May include Mn-rich quartzites found overlying amphibolites.|
5300|Dean Quartzite|70018|4|Described|p234-240|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the southern Amadeus Basin. Correlable to Heavitree Quartzite in the northern Amadeus Basin. Deposition occurred during post-rift subsidence after initial uplift of Musgrave Block in a braod intracratonic basin between Musgrave Block and Arunta region. Thinly to thickly bedded (50-100m) and crops out in the southwestern Amadeus Basin where it commonly forms prominent ridges and escarpments. Zircon data show two broad peaks representing a mixture between sediments derived from the Musgrave Block and Arunta Region.||||Overlain by Pinyanna Beds. Underlain by Kulail Sandstone.|Massive, clean, white, schistose sericitic quartzite.|
5300|Dean Quartzite|70416|5|Briefly described|p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||Correlated with Heavitree Quartzite.||
5300|Dean Quartzite|70634|4|Described|500k_geolgyp08_lut.csv|Neoproterozoic|Neoproterozoic|Included with Heavitree Quartzite in file (undivided).|||||Quartz sandstone, sandstone, and conglomerate; kyanite schist locally.|
5300|Dean Quartzite|70793|4|Described|500k_interpgeop14_lut.csv + geochron|Cryogenian|Neoproterozoic|Of Amadeus Basin (Phase 1), Centralian Superbasin. Occurs on the SW margin of the Amadeus Basin. Events: Alice Springs Orogeny (450-295 Ma); Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199404 (quartzite) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1120+\-29 Ma. See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred; biostrat).|||Underlain by Kulail Sandstone. Equivalent to Heavitree Quartzite.|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
5300|Dean Quartzite|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
5300|Dean Quartzite|70839|5|Briefly described|p328-334,336|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Basal unit of Supersequence 1; Equivalent to Kulail Sandstone, and Heavitree Quartzite to the north. Exposed as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Detrital zircon age spectrum range between c. 2.8 and 1.04 Ga; major late paleoproterozoic age component at c. 1.88-1.62 Ga (peaks at c. 1.69 and 1.73 Ga) and major Mesoproter0zoic age component between 1.35 and 1.04 Ga (Warakurna Supersuite). Peaks at 1.2 [derived from Pitjantjatjara Supersuite; Musgrave orogeny] and 1.31 Ga [Wankanki Supersuite; Giles event]). Minor peaks at c. 2.8, 2.5 and 2.4 Ga, and a small age cluster between c. 1.48 and 1.4 Ga (Papulankutja Supersuite, west Musgrave).|Max dep age: 1039+\-35 Ma (207Pb/206Pb)|||Overlain by Bitter Springs Formation or Pinyanna beds. Correlable to Kulail Sandstone and Heavitree Quartzite.||
5300|Dean Quartzite|71080|5|Briefly described|p23, p29 Fig 20, p30|Tonian|Tonian|Southern Amadeus Basin. Supersequence 1.||||Correlated with Heavitree Formation, Amadeus Basin; Munyu Sandstone, Murraba Basin.|Dominantly sandstone.|
5300|Dean Quartzite|71088|6|Mentioned|p6, p8, p10, p17|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Part of Supersequence 1.|c. 1200-1150 Ma|||||
5300|Dean Quartzite|71170|5|Briefly described|p114, p122|Mesoproterozoic|Mesoproterozoic|15m thick sequence directly above basement. Metamorphic muscovite is dated at 598 +/- 3 Ma. P-T conditions during metamorphism are estimated.|||||Fine-medium grained quartzite.|
5300|Dean Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, schist, sandstone, quartzite|
5300|Dean Quartzite|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199404 (quartz-rich sandstone) yielded a weighted mean 207Pb/206Pb age of 1120+\-29 Ma, interpreted as maximum depositional age of sandstone. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|976-827 Ma (inferred)|||Overlain by Bitter Springs Group. Underlain by  Kulail Sandstone. Correlable with Heavitree Quartzite, Vaughan Springs Quartzite.|Fine- to coarse-grained, white to grey-blue paraquartzite; commonly thickly bedded and devoid of sedimentary structures; locally contains heavy mineral bands; sandstone, lesser siltstone and conglomerate; commonly intensely silicified.|
5300|Dean Quartzite|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
5300|Dean Quartzite|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1120+/-29 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained quartz sandstone.|
5300|Dean Quartzite|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||Equivalent to Heavitree Formation. Overlain by Pinyanna beds or Gillen Formation. Underlain by and grades into Kulail Sandstone or basement.||
5300|Dean Quartzite|71842|5|Briefly described|p2-3|Cryogenian|Cryogenian|Of Amadeus Basin.||||Overlain by Bitter Springs Group. Correlable to Heavitree Quartzite.||
5300|Dean Quartzite|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Informal grouping of mostly time-equivalent silicilastic units. Grouped with Kulail Sandstone, Heavitree Quartzite, and Vaughan Springs Quartzite. Min age  from biostratigraphy.|||||Informal grouping description: Quartz sandstone, sandstone, and conglomerate; kyanite schist locally [probably only in Dean Quartzite].|
5300|Dean Quartzite|72094|5|Briefly described|p3 Fig 2, p7|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Strongly folded ridges of Dean Quartzite interleaved with Tjauwata Group rhyolite-dominant rocks.||
5300|Dean Quartzite|72375|4|Described|p5|Tonian|Stenian|Of Amadeus Basin. Inferred max depositional age of c. 1040-820 Ma, based on age of underlying Tjauwata Group (c. 1090-1040 Ma; Close et al., 2005), and the similar geochemical affinities with Johnnys Creek Formation basalts and the c. 824 Ma Amata Dolerite. ||||Underlain by Tjauwata Group. Correlable with Heavitree Formation.||
5300|Dean Quartzite|72601|6|Mentioned|p3|Tonian|Tonian|Amadeus Basin. Found in the southern part of the basin.||||Overlain by Gillen Formation (Bitter Springs Group).||
5300|Dean Quartzite|73085|6|Mentioned|p1|Tonian|Tonian|||||Partly underlain by Kulail Sandstone. Partly overlain by Pinyinna beds and Gillen Formation (Bitter Springs Group). Equivalent to Heavitree Formation.||
5300|Dean Quartzite|73086|6|Mentioned|p3, p7, p9, p15, p18, p145|||Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Restricted to exposures in the southwest of the basin. Exposed for ~400 km along the south-western margin of the basin.||||Correlates to Heavitree Formation. Conformably overlain by Pinyinna beds.||
5300|Dean Quartzite|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Equivalent to Heavitree Quartzite, conformably underlies the Bitter Springs Group and Gillen Formation.||
5300|Dean Quartzite|73346|6|Mentioned|p2, p5, p14|Tonian|Tonian|Amadeus Basin. Outcrops of sandstone originally assigned to this unit east of the Giles Mulga Park Road [in the Cobb Embayment] were reinterpreted as the basal succession of the Cobb Formation.||||||
5300|Dean Quartzite|73437|6|Mentioned|p151-152|Neoproterozoic|Neoproterozoic|Amadeus Basin. (U-Th)/He zircon cooling ages of 531+/-72 Ma and 546+/-52 Ma. K-Ar muscovite cooling ages of 568+/-5 Ma and 586+/-5 Ma from Scrimgeour et al., (1999).||||||
5384|Depot Granodiorite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Hornblende-granodiorite and tonalite with scattered microcline phenocrysts|
5384|Depot Granodiorite|23786|5|Briefly described|p34 Tb. 4|||Geological Province: Yilgarn Craton.||||||
5384|Depot Granodiorite|41914|4|Described|p21|||||||||
5384|Depot Granodiorite|42626|6|Mentioned|p38|||||||||
5384|Depot Granodiorite|42698|5|Briefly described|map legend|||||||||
5384|Depot Granodiorite|42892|4|Described|p43|||||||||
5384|Depot Granodiorite|60076|5|Briefly described|p45 App. 1|||[Aggde]   Medium- to coarse-grained hornblende leuco-granodiorite-tonalite.||||||13-APR-05
5384|Depot Granodiorite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium- to coarse-grained, hornblende leucogranodiorite-leucotonalite; foliation moderate except in numerous shear zones; intrusive western contact.||||||07-FEB-11
5384|Depot Granodiorite|68066|5|Briefly described|p16, p27-29, p31, map|Archean|Archean|Ovoid (10 x 20 km) body. Folded and foliated greenstones wrap around the margins of this mass.||||Truncated by Celebration Dyke on northern margin.|Medium to coarse grained, hornblende bearing leuco-granodiorite to leuco-tonalite, with polygonal to interlobate granoblastic texture, and scattered microcline phenocrysts in a streaky granular matrix.|
5384|Depot Granodiorite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium- to coarse-grained, hornblende leucogranodiorite-leucotonalite; foliation moderate except in numerous shear zones; intrusive western contact.|05-AUG-15
5384|Depot Granodiorite|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].||||||
5384|Depot Granodiorite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Medium- to coarse-grained, hornblende leucogranodiorite and leucotonalite; foliation moderate except in numerous shear zones; intrusive western contact; metamorphosed.|
5384|Depot Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite, granodiorite|
5384|Depot Granodiorite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). Oval granotic pluton, exposed over an area of 16x12 km2. Shows solid-state deformation fabric at the margins. Sample GSWA 182288 (metagranodiorite) yielded a weighted mean 207Pb/206Pb date of 2689+\-3 Ma, interpreted as the igneous crystallization age of the granodiorite. See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|1689+\-3 Ma (inferred)|||Intrudes into Black Flag Group. Intuded by pegmatite dykes.|Medium- to coarse-grained, hornblende leucogranodiorite and leucotonalite; metamorphosed|
5416|Desirable Pillow Lava Member|30562|4|Described|p37|||||||||
5416|Desirable Pillow Lava Member|42626|6|Mentioned|Fig.4 P10|||||||||
5433|Devils Elbow No.3 kimberlite|41158|6|Mentioned|p68|||||||||
5437|Devon Consols Basalt|22534|6|Mentioned|Fig.5 p10|||Of Kalgoorlie Group.||||||14-APR-08
5437|Devon Consols Basalt|22666|5|Briefly described|p696, Fig.1b|||||||||
5437|Devon Consols Basalt|23137|4|Described|p245 Table.2|||Of Kalgoorlie Group.||||||14-APR-08
5437|Devon Consols Basalt|23139|4|Described|p234 Fig.2, p235|||||||||
5437|Devon Consols Basalt|23786|5|Briefly described|p10|Archean|Archean|Of Kambalda Group.  Geological Province: Yilgarn Craton.||||||07-NOV-08
5437|Devon Consols Basalt|23924|5|Briefly described|p205|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
5437|Devon Consols Basalt|23926|5|Briefly described|p17|||||||||
5437|Devon Consols Basalt|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
5437|Devon Consols Basalt|24139|5|Briefly described|p239 Table 1|Archean|Archean|Geological Province: Kambalda Domain. Of the Kalgoorlie Group.||||||07-NOV-08
5437|Devon Consols Basalt|24322|5|Briefly described|p61 Fig. 2|Archean|Archean|Of the Kambalda Group.||||||07-NOV-08
5437|Devon Consols Basalt|24325|5|Briefly described|p61 Fig. 2|||Of the Kambalda Group. Overlain by the Kapai Slate. Overlies the Kambalda Komatiite Formation. Geological Province: Kambalda Dome, Yilgarn Craton.||||||
5437|Devon Consols Basalt|29418|6|Mentioned|p116|||||||||
5437|Devon Consols Basalt|29681|5|Briefly described|Table 2|||||||||
5437|Devon Consols Basalt|29784|6|Mentioned|Table 1|||||||||
5437|Devon Consols Basalt|30779|6|Mentioned|Table 1|||Stratigraphy||||||
5437|Devon Consols Basalt|30886|6|Mentioned|Table 4|||||||||
5437|Devon Consols Basalt|30900|6|Mentioned|p67|||On Table 1||||||
5437|Devon Consols Basalt|31042|6|Mentioned|Fig. 4|||Correlation||||||
5437|Devon Consols Basalt|32685|5|Briefly described|Table 1|||||||||
5437|Devon Consols Basalt|33515|6|Mentioned|p33|||||||||
5437|Devon Consols Basalt|33535|4|Described|p177|||||||||
5437|Devon Consols Basalt|34608|6|Mentioned|p2|||||||||
5437|Devon Consols Basalt|35611|6|Mentioned|Fig.2|||Stratigraphic columns for Kalgoorlie and Kambalda.||||||
5437|Devon Consols Basalt|36869|6|Mentioned|p48|||||||||
5437|Devon Consols Basalt|39046|6|Mentioned|Fig.2|||||||||
5437|Devon Consols Basalt|39895|5|Briefly described|Fig.1|||||||||
5437|Devon Consols Basalt|40005|6|Mentioned|Fig.16|||||||||
5437|Devon Consols Basalt|40083|6|Mentioned|p118|||See also Fig.2||||||
5437|Devon Consols Basalt|40849|6|Mentioned|p37|||||||||
5437|Devon Consols Basalt|41066|6|Mentioned|1 of 2 L17|||||||||
5437|Devon Consols Basalt|41249|6|Mentioned|p4|||||||||
5437|Devon Consols Basalt|41368|6|Mentioned|Fig.1|||||||||
5437|Devon Consols Basalt|41379|6|Mentioned|p40|||||||||
5437|Devon Consols Basalt|41458|6|Mentioned|p361|||||||||
5437|Devon Consols Basalt|41588|4|Described|p244|||||||||
5437|Devon Consols Basalt|41644|6|Mentioned|p219|||||||||
5437|Devon Consols Basalt|41771|6|Mentioned|Fig.3|||||||||
5437|Devon Consols Basalt|41784|6|Mentioned|p65|||||||||
5437|Devon Consols Basalt|41889|6|Mentioned|Fig.1|||||||||
5437|Devon Consols Basalt|41890|5|Briefly described|p278|||||||||
5437|Devon Consols Basalt|42117|5|Briefly described|Table 1 P67|||||||||
5437|Devon Consols Basalt|42160|6|Mentioned|p46|||||||||
5437|Devon Consols Basalt|42195|6|Mentioned|Fig.4 P147|||||||||
5437|Devon Consols Basalt|42221|6|Mentioned|Table 1 P6|||||||||
5437|Devon Consols Basalt|42406|5|Briefly described|Fig.2 P250|||||||||
5437|Devon Consols Basalt|42696|6|Mentioned|Plate 1B|||||||||
5437|Devon Consols Basalt|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
5437|Devon Consols Basalt|42817|5|Briefly described|Fig.3|||||||||
5437|Devon Consols Basalt|42870|5|Briefly described|Table 1, P67|||||||||
5437|Devon Consols Basalt|42892|6|Mentioned|Table 3|||||||||
5437|Devon Consols Basalt|42969|6|Mentioned|Fig.1 p106|||||||||
5437|Devon Consols Basalt|43102|5|Briefly described|p8|||||||||
5437|Devon Consols Basalt|43162|6|Mentioned|5|||||||||
5437|Devon Consols Basalt|43496|5|Briefly described|6-15|||||||||03-MAR-10
5437|Devon Consols Basalt|44149|6|Mentioned|p88 fig 2-90, p91 tab 2-9|Archean|Archean|Kalgoorlie area, Eastern Goldfields Province.||||||
5437|Devon Consols Basalt|45546|14|Not recorded|p.50-52|||||||||
5437|Devon Consols Basalt|46905|5|Briefly described|Table 1|||Stratigraphic succession.||||||21-OCT-08
5437|Devon Consols Basalt|50556|5|Briefly described|p1116 Fig.6||Archean|Overlies Kambalda Komatiite. Eastern Goldfields Province.||||||07-NOV-08
5437|Devon Consols Basalt|50622|6|Mentioned|p316 Fig.3|||||||||
5437|Devon Consols Basalt|60076|5|Briefly described|p12 Tb. 2|||Variolitic high-Mg basalt.  Max. thickness: 300m. Geological Province: Kambalda domain.||||||14-APR-08
5437|Devon Consols Basalt|60514|4|Described|p27 Fig. 4, p29, p41 Fig. 11, p65 Tb. 1|Archean|Archean|Of Kalgoorlie Group. Overlain by Kapai Slate, underlain by Tripod Hill Member of the Kambalda Komatiite. Age: 2693+/-30 Ma. Max thickness: 150m. Consists of pillowed + massive  lava flows + thin dolerites. Geol Prov: Kambalda Domain, Yilgarn Craton.||||||11-OCT-12
5437|Devon Consols Basalt|60555|6|Mentioned|p5, p6 Fig. 3|Archean|Archean|Underlain by Kambalda Komatiite, overlain by Kapai Slate.||||||07-NOV-08
5437|Devon Consols Basalt|60578|6|Mentioned|p6 Fig.1|Archean|Archean|||||||07-NOV-08
5437|Devon Consols Basalt|60623|4|Described|p25 Fig.2, p28|Archean|Archean|Age: 2693+/-30 Ma. Conformably overlies Tripod Hill Member of Kambalda Komatiite. Max. thickness: >150m. Divided geochemically into high Si, low Mg basalts and low Si, high Mg basalts. Of Kalgoorlie Group. Geological Province: Eastern Goldfields.||||||07-NOV-08
5437|Devon Consols Basalt|60626|6|Mentioned|p55 Fig.2|||||||||
5437|Devon Consols Basalt|60627|5|Briefly described|p65 Tb.1|||Of Kalgoorlie Group.||||||
5437|Devon Consols Basalt|61855|6|Mentioned|p333|||||||||
5437|Devon Consols Basalt|62108|5|Briefly described|p1409 Tb. 6|Archean|Archean|Of the Kalgoorlie Group. High Mg variolitic basalt. Age: 2693+/-30Ma. Max. thickness: 100m. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1417 Fig. 10, p1420 Fig. 14.||||||07-FEB-11
5437|Devon Consols Basalt|62109|5|Briefly described|p1428, p1429 Fig. 2|||Pillowed to massive magnesian lavas. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton.||||||14-APR-08
5437|Devon Consols Basalt|62110|5|Briefly described|p1442 Fig. 1|||Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
5437|Devon Consols Basalt|62111|5|Briefly described|p1458 Fig. 2|||Of the Kambalda Group. Geological Province: Kambalda Dome in the Norseman-Wiluna greenstone belt of the Yilgarn Craton.||||||07-FEB-11
5437|Devon Consols Basalt|62406|6|Mentioned|p54 Fig. 2|||||||||
5437|Devon Consols Basalt|64016|6|Mentioned|p56|||Thickness: 60 to 200m. Consists of high magnesium basalt with a pillowed to massive structure and variolitic texture.||||||19-JUN-08
5437|Devon Consols Basalt|64340|6|Mentioned|p7|||Underlain by Kapai Slate. ||||||
5437|Devon Consols Basalt|64715|5|Briefly described|p3, p4, p5 Fig. 4|||Overlain by Kapai Slate. Contains detrital zircons with age: c.2692Ma at Kambalda (Claoue-Long et al, 1988). Pillow basalt east of the headland islands in Hannan Lake. See also p6, p7 Fig. 7.||||||16-DEC-08
5437|Devon Consols Basalt|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Kambalda Domain. Komatiitic basalt.||||||
5437|Devon Consols Basalt|65834|6|Mentioned|p7, 44-45, 47, 53-57, 62|||Kambalda Domain, Kalgoorlie Terrane. Hosts gold mineralisation.||Kalgoorlie Group.||||
5437|Devon Consols Basalt|66854|5|Briefly described|p944, p946 Fig.3. |||Forms part of the core of the Kambalda Anticline.||||Overlies Kambalda Komatiite.||
5437|Devon Consols Basalt|66880|6|Mentioned|p7, |Archean|Archean|||Unit in Kambalda Sequence.||Overlies Kambalda Komatiite. Is overlain by Kapai Slate.||
5437|Devon Consols Basalt|67020|6|Mentioned|p660.|Archean|Archean|||||Overlies Kambalda Komatiite Formation. Is overlain by Kapai Slate.||
5437|Devon Consols Basalt|67198|4|Described|p5 Fig.2, p81, p83, p94, p114, p118-119|Neoarchean|Neoarchean|60-100m thick. Also referred to as D.C. Basalt in Fig.2 and Devon Consuls Basalt on p83 and p88. Kalgoorlie Terrane. Basalts divided into two geochemical groups. SHRIMP crystallisation age. Has xenocrystic zircons with >3.4 Ga cores.|2693 +/- 50 Ma (Compston et al, 1986)|Kambalda Sequence||Overlies Kambalda Komatiite, Tripod Hill Member overlain by Kapai Slate, Paringa Basalt, Intruded by Kambalda Granodiorite, faulted against Tripod Hills Komatiite.|Pillowed basalt flows with felsic ocelli and massive komatiitic basalt with minor pillowed phases.|11-SEP-17
5437|Devon Consols Basalt|68110|6|Mentioned|p685|||Discussed in the context of crustal contamination.||||||
5437|Devon Consols Basalt|68216|6|Mentioned|p301 Fig. 1|||SH51-9||||||
5437|Devon Consols Basalt|68217|4|Described|p71, 73, 75|Precambrian||Approx 200-500 ft thick [61-153m thick]||||Overlain by Kapai Slate. Underlain by Hannans Lake Serpentinite.|Meta-basaltic lavas, typically pillow lavas.|02-MAY-16
5437|Devon Consols Basalt|68289|5|Briefly described|p6-p7, p11-p13, p29-p31|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. 50-500m thick. Outcrop localities are provided.||||Overlies the Kambalda Komatiite (Tripod Hill Member). Overlain by the Kapai Slate. Intruded by the Kambalda Granodiorite.|Variolitic basalt with well-preserved pillow structures.|
5437|Devon Consols Basalt|69035|5|Briefly described|pp413-415 Fig.1, p424, p429|||~ 200 m thick. Basal olivine basalt flows gradational to Hannans Lake Serpentinite.|||||Comprises high magnesian basalts; variolitic textured, pillowed to massive with minor intercalated pyritic graphitic mudstones.|01-JUL-14
5437|Devon Consols Basalt|69583|6|Mentioned|p37|||Southern Kalgoorlie Terrane. 50-500m thick.||||||
5437|Devon Consols Basalt|69619|6|Mentioned|p115|||||||Overlies Kambalda Komatiite. Is overlain by Paringa Basalt.||
5437|Devon Consols Basalt|69631|5|Briefly described|p7, p11, p14-16, p25, p28|||Kambalda area, Kalgoorlie Terrane. 50-500m thick. Forms rubbly outcrops. Mis-spelt as Devons Consol Basalt on p25.||||Overlies Kambalda Komatiite. Is overlain by Kapai Slate.|Variolitic basalt with well-preserved pillow structures. Deformed by regional metamorphism.|
5437|Devon Consols Basalt|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2792 - 2692 Ma (inferred).|Hannans Subgroup|||Komatiitic basalt; massive to variolitic; locally pillowed; metamorphosed. Shale with fine-grained laminated siltstone and chert, minor sandstone; metamorphosed.|
5437|Devon Consols Basalt|70287|6|Mentioned|p188, 190|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton.|2690 +/- 5 Ma (Claoue-Long et al., 1998).|||Overlies Kapai Slate. Is overlain unconformably by Black Flag Beds.||
5437|Devon Consols Basalt|70290|6|Mentioned|p296-298|||Kalgoorlie district, Yilgarn Craton.||||Is overlain by Williamstown gabbro.|High-Mg pillow basalt. Greenschist facies metamorphism.|
5437|Devon Consols Basalt|70326|5|Briefly described|p335,360-363|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. LREE-enriched basalts (Clout, 1991). Correlable to Redeemer Basalt.|c. 2690 Ma (Clout, 1991)|||Overlain by Paringa Basalt. Underlain by Kambalda Komatiite and Lunnon Basalt. Intruded by Victory Dolerite.||
5437|Devon Consols Basalt|70773|5|Briefly described|p18 fig 11, p21, p22, p24 fig 16|Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane.|c. 2700 Ma|Kambalda Sequence||Overlies the Kambalda Komatiite. Overlain by the Paringa Basalt or the Kapai Slate.|Basalt.|
5437|Devon Consols Basalt|70863|6|Mentioned|p9|||Kambalda Dome, Yilgarn Craton.||||||
5437|Devon Consols Basalt|71148|6|Mentioned|p122, 130-131, 135|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton. Often abbreviated to D.C. basalt. Geochemistry detailed.|2687 +/- 4 Ma.|Kambalda Sequence.||||
5437|Devon Consols Basalt|71166|6|Mentioned|p119 fig 3.89|||||||||
5437|Devon Consols Basalt|71270|4|Described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).|2702-2692 Ma (inferred)|Unit of Hannans Subgroup.|||Komatiitic basalt; massive to variolitic; locally pillowed; metamorphosed; Shale with fine-grained lamined siltstone and chert; minor sandstone; metamorphosed.|
5437|Devon Consols Basalt|71308|5|Briefly described|p711, p714|||Archibald et al. (1978). Southern Kalgoorlie Terrane. Said to be the "type" stratigraphic unit for the authors' Intermediate-Th Basalts group. Geochemistry discussed in detail.|2700 Ma.|Kambalda Sequence.||||
5437|Devon Consols Basalt|71309|6|Mentioned|p740 Fig.3|||Appears as D.C. Basalt in Fig.3.||||||
5437|Devon Consols Basalt|72049|6|Mentioned|p259-p260|||Kalgoorlie Terrane.||Kambalda Sequence||||
5437|Devon Consols Basalt|72095|4|Described|p4, p6-17,21|||Eastern Goldfields, Yilgarn Craton. Basement to the Kalgoorlie-Kambalda region. Extensively intruded by mafic and ultramafic sills. Detailed geochemistry is described.||Unit of Hannans Subgroup.||At a stratigraphic position consistent with  a sequence of flow units of Intermediate-Th Basalt (ITB; Barnes et al., 2012) composition that overlies Kambalda Komatiite. Overlain by Kapai Slate.||
5437|Devon Consols Basalt|73300|6|Mentioned|p1112-1113, p1118 Fig.7|||Yilgarn Craton, Kalgoorlie terrane.||Kambalda Sequence||Overlies the Hannan's Lake Serpentinite, underlies the Kapai Slate.||
5437|Devon Consols Basalt|73391|5|Briefly described|p19, 24, 114, 194, 206, 238, 244, 279|||See also p304, 306, 308, Appendices. Woodall (1965). Kambalda Domain, Kalgoorlie Terrane. 60-100m thick. Occurs only as DCB in the stratigraphic column on p194.|<2692 +/- 4 Ma.|||Overlies Kambalda Komatiite. Is overlain by Kapai Slate.|Basaltic pillowed lava. Associated with komatiites.|
5437|Devon Consols Basalt|73596|6|Mentioned|p1160, 1162|||Appears as Devon Consol/Bent Tree Basalt on p1160.||Hannans Subgroup.||Overlies Kambalda Komatiite. Is overlain by Kapai Slate.||
5459|Dick Creek Dolomite|37371|6|Mentioned|p363|||||||||
5507|Dingo Claystone|6876|6|Mentioned|p100 Fig.5.|Jurassic|Jurassic|Equivalent units are shown on the diagram.||||||
5507|Dingo Claystone|12466|5|Briefly described|p173, pp176-177.|Late Jurassic|Late Jurassic|Westralian 2 (W2) oils source rock for Barrow and Dampier Sub-basin oils; hydrocarbons generated from mixed terrestrial and marine organic matter in a clastic marine setting.||||Overlies Mungaroo Formation.||22-FEB-13
5507|Dingo Claystone|12471|6|Mentioned|p475 Fig.2. |Late Jurassic|Early Jurassic|Fine-grained siliciclastics. See also Figs 4, 6.||||||27-OCT-14
5507|Dingo Claystone|12491|4|Described|pp447-449, p463.|Late Jurassic|Late Jurassic|2 km thick. Principal oil source in Northern Carnarvon Basin. Most oils can be correlated to W.spectabilis biozone within the Oxfordian. Deposited in low-energy, open marine, locally anoxic, troughs. Minimum of three phases of hydrocarbon migration. Dingo Formation used in figures. Dingo Claystone used in text.||||Overlies Calypso Formation. Is overlain by Dupuy Formation.|Marine claystones and sporadic siltstones.|27-OCT-14
5507|Dingo Claystone|12498|6|Mentioned|p517 Fig.3. |Late Jurassic|Late Jurassic|||||Overlies Calypso Formation.||
5507|Dingo Claystone|12525|6|Mentioned|p45.|Late Jurassic|Late Jurassic|Oxfordian-Kimmeridgian. North West Cape. Intruded by sills.||||||
5507|Dingo Claystone|13255|6|Mentioned|p364|Late Jurassic|Late Jurassic|Carnarvon Basin.||||||
5507|Dingo Claystone|13615|3|Fully described|p3-p4, p6-p8, p18, p27|Tithonian|Hettangian|Peedamullah Shelf. Reaches >1500m thick offshore. Spores/Pollen Zone and Dinoflagellate zones provided. Up to 1405.5 m thick. Deposited as a basinal marine formation. Type section occurs in Barrow Deep 1 between 2177 and 3229m. Deposited in a low energy marine environment. See also p35, p43, p79, p82, p102 App. 3, p118 App5,  Plates 2, 3.|c. 159 Ma|||Conformably overlies the Mungaroo Formation. Unconformably overlain by the Flacourt Formation.|Grey clayey siltstone, lesser claystone and some sandstone.|07-FEB-19
5507|Dingo Claystone|22703|4|Described|p115,118-9,Fig.3|Tithonian|Callovian|||||||
5507|Dingo Claystone|23379|4|Described|p160 Fig.2;p158, 164, 167|Tithonian|Callovian|Of Barrow Sub-basin, Carnarvon Basin.||||||01-OCT-08
5507|Dingo Claystone|23726|5|Briefly described|p91|Jurassic|Jurassic|Underlying unit Athol Formation. Geological Province: Carnarvon Basin.||||||
5507|Dingo Claystone|23815|4|Described|p292|Early Jurassic|Early Jurassic|Geological Province: Barrow Sub-basin. Overlain by Barrow Formation (unconformable). Underlain by Mungaroo Formation. Max. thickness: 802 m. Fossiliferous.||||||18-JAN-07
5507|Dingo Claystone|24059|5|Briefly described|p131|Jurassic|Jurassic|Geological Province: Barrow Sub-basin.||||||
5507|Dingo Claystone|24084|5|Briefly described|p146 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: North Carnarvon Basin.||||||16-MAR-05
5507|Dingo Claystone|24246|6|Mentioned|p19|||Geological Province: Carnarvon Basin.||||||
5507|Dingo Claystone|24331|5|Briefly described|p475 Fig.2|Late Jurassic|Early Jurassic|Overlies Brigadier Formation (conformable) and Mungaroo Formation (unconformable). Overlain conformably by Dupuy Formation. Marine. Geological Province: Barrow Sub-basin.||||||
5507|Dingo Claystone|24351|5|Briefly described|p16, p39, Plate 4 (in pocket)|Late Jurassic|Middle Jurassic|Geological Province: Exmouth Sub-basin. Marine shales and siltstones. Considered to be a rich source rock for oil.||||||13-DEC-07
5507|Dingo Claystone|24390|5|Briefly described|p21|Late Jurassic|Late Jurassic|Geological Province: Northern Carnarvon Basin.||||||
5507|Dingo Claystone|30110|6|Mentioned|p84|||Upper Jurassic age.||||||
5507|Dingo Claystone|30304|3|Fully described|p51|||Late Jurassic age||||||
5507|Dingo Claystone|30365|6|Mentioned|Fig.8|||||||||
5507|Dingo Claystone|30693|6|Mentioned|p63|||||||||
5507|Dingo Claystone|31083|6|Mentioned|p456|||||||||
5507|Dingo Claystone|31561|5|Briefly described|p34|||See also P37. Early - Mid Juurassic.||||||
5507|Dingo Claystone|32642|6|Mentioned|p76|||Gas & condensate encountered||||||
5507|Dingo Claystone|32648|6|Mentioned|p32|||Jur.||||||
5507|Dingo Claystone|32712|6|Mentioned|Table 1|||||||||
5507|Dingo Claystone|32715|6|Mentioned|p1177|||||||||
5507|Dingo Claystone|33166|6|Mentioned|p66|||Stratigraphy||||||
5507|Dingo Claystone|33386|6|Mentioned|Fig.7|||||||||
5507|Dingo Claystone|33435|6|Mentioned|p134|||Jurassic.||||||
5507|Dingo Claystone|33453|4|Described|p71|||Jurassic.||||||
5507|Dingo Claystone|33622|4|Described|p92|||||||||
5507|Dingo Claystone|33627|6|Mentioned|p582|||||||||
5507|Dingo Claystone|33813|6|Mentioned|p5|||See also Figs 5 & 6||||||
5507|Dingo Claystone|34008|6|Mentioned|p72|||Jurassic||||||
5507|Dingo Claystone|34134|6|Mentioned|Cor.Chart|||Lower - Upper Jurassic||||||
5507|Dingo Claystone|34363|6|Mentioned|p56|||Middle - Upper Jurassic. See also Fig.7.||||||
5507|Dingo Claystone|34840|6|Mentioned|p66|||||||||
5507|Dingo Claystone|34846|6|Mentioned|Fig.3|||||||||
5507|Dingo Claystone|35282|6|Mentioned|Fig.2|||||||||
5507|Dingo Claystone|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
5507|Dingo Claystone|35983|6|Mentioned|Table 27|||||||||
5507|Dingo Claystone|36093|6|Mentioned|Fig.2|||||||||
5507|Dingo Claystone|36112|6|Mentioned|p29|||||||||
5507|Dingo Claystone|36257|6|Mentioned|Table 2.1|||||||||
5507|Dingo Claystone|36266|6|Mentioned|p152|||||||||
5507|Dingo Claystone|36890|3|Fully described|p292|||||||||
5507|Dingo Claystone|37320|6|Mentioned|p235|||||||||
5507|Dingo Claystone|37364|6|Mentioned|p1050|||||||||
5507|Dingo Claystone|37577|6|Mentioned|p77|||||||||
5507|Dingo Claystone|37689|6|Mentioned|p25|||On schematic section.||||||
5507|Dingo Claystone|39427|4|Described|Table 1|||||||||
5507|Dingo Claystone|39486|6|Mentioned|p2091|||||||||
5507|Dingo Claystone|39757|6|Mentioned|p1605|||||||||
5507|Dingo Claystone|40617|6|Mentioned|p7|||||||||
5507|Dingo Claystone|40992|6|Mentioned|Fig.8|||||||||
5507|Dingo Claystone|41170|6|Mentioned|p155|||||||||
5507|Dingo Claystone|41271|3|Fully described|p121|||||||||
5507|Dingo Claystone|41436|6|Mentioned|p45|||||||||
5507|Dingo Claystone|41438|6|Mentioned|p108|||||||||
5507|Dingo Claystone|41439|4|Described|p116|||||||||
5507|Dingo Claystone|41440|4|Described|p136|||||||||
5507|Dingo Claystone|41441|6|Mentioned|p153|||||||||
5507|Dingo Claystone|41443|5|Briefly described|p166|||||||||
5507|Dingo Claystone|41446|6|Mentioned|Fig.2|||||||||
5507|Dingo Claystone|41589|6|Mentioned|p118|||||||||
5507|Dingo Claystone|41709|6|Mentioned|p213|||||||||
5507|Dingo Claystone|41716|6|Mentioned|p335|||||||||
5507|Dingo Claystone|41732|6|Mentioned|p534|||||||||
5507|Dingo Claystone|41751|3|Fully described|p3|||||||||
5507|Dingo Claystone|42075|5|Briefly described|Fig.4 P245|||||||||
5507|Dingo Claystone|42116|5|Briefly described|p70|||||||||
5507|Dingo Claystone|42150|6|Mentioned|p66|||||||||
5507|Dingo Claystone|42463|6|Mentioned|Fig.2 P169|||||||||
5507|Dingo Claystone|42598|6|Mentioned|p90, p55|||||||||
5507|Dingo Claystone|42615|3|Fully described|p35||Oxfordian|||||||
5507|Dingo Claystone|43710|6|Mentioned|p31|||||||||
5507|Dingo Claystone|43712|5|Briefly described|p11||Jurassic|||||||
5507|Dingo Claystone|43722|5|Briefly described|p10||Jurassic|||||||
5507|Dingo Claystone|43724|4|Described|p29||Jurassic|||||||
5507|Dingo Claystone|43824|6|Mentioned|p137|||||||||
5507|Dingo Claystone|43826|6|Mentioned|Fig.2,p163|Late Jurassic|Early Jurassic|||||||01-MAR-10
5507|Dingo Claystone|44998|14|Not recorded|App.5 p289|||||||||
5507|Dingo Claystone|45015|5|Briefly described|map legend|Late Jurassic|Middle Jurassic|Formation known only in bores. Geological Province: Carnarvon Basin.||||||31-MAY-06
5507|Dingo Claystone|45142|6|Mentioned|Fig.4|||||||||
5507|Dingo Claystone|46808|6|Mentioned|Table 2|||||||||
5507|Dingo Claystone|49942|5|Briefly described|p39|Late Jurassic|Late Jurassic|Geological Province: Northern Carnarvon Basin. Oil source rock.||||||
5507|Dingo Claystone|50025|5|Briefly described|p12|||Underlies the Macedon Member. Forms seal for sandstone reservoirs in Mungaroo Formation. Geological Province: Exmouth Sub-basin.||||||17-SEP-14
5507|Dingo Claystone|50085|5|Briefly described|p23 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin.||||||
5507|Dingo Claystone|60376|6|Mentioned|p23, p29.|||Geological Province: Carnarvon Basin.||||||07-FEB-11
5507|Dingo Claystone|60379|6|Mentioned|p126 fig 3, p127|Kimmeridgian|Kimmeridgian|Dampier sub-basin, Carnarvon Basin. Petroleum source rocks, generally immature. Age stated in text, but Fig 3 suggests minimum age may be Tithonian.||||||
5507|Dingo Claystone|60384|6|Mentioned|p244, p243 Fig 2b, p261|Late Jurassic|Early Jurassic|Exmouth Sub-basin, Northern Carnarvon Basin. Two different ages given.  Table says Late Jurassic, p244 implies Early.||||||
5507|Dingo Claystone|60386|6|Mentioned|p300, 302|Early Cretaceous|Middle Jurassic|Northern Carnarvon Basin. Distal shelf/basin.||||||
5507|Dingo Claystone|61023|5|Briefly described|p27 Fig. 12|Jurassic|Jurassic|Geological Province: Northern Carnarvon Basin. See also p29.||||||10-APR-08
5507|Dingo Claystone|61554|6|Mentioned|p625 Fig.2|||Barrow Island.||||||
5507|Dingo Claystone|61555|5|Briefly described|p236, 237|Kimmeridgian|Oxfordian|Exmouth Sub-basin, Barrow Sub-basin. Widespread marine claystone. Up to 3000 m thick. Hydrocarbon source rocks.||||Is overlain by Dupuy Formation.||20-MAR-12
5507|Dingo Claystone|61958|5|Briefly described|Map sheet 1|Late Jurassic|Middle Jurassic|||||||
5507|Dingo Claystone|62837|5|Briefly described|Stratigraphic columns|Middle Jurassic|Middle Jurassic|Age: >160-150Ma. Geological Province: Northern Carnarvon Basin.||||||01-MAR-10
5507|Dingo Claystone|63950|5|Briefly described|p336 Fig. 4, p334, p337|Early Cretaceous|Late Jurassic|Overlies Calypso Formation. Geological Province: northern Carnarvon Basin.||||||01-FEB-10
5507|Dingo Claystone|64977|6|Mentioned|p493 Fig.3.|Late Jurassic|Early Jurassic|Thevenard Island area.||||Unconformably overlies Mungaroo Formation. Is overlain by Dupuy Formation.||
5507|Dingo Claystone|64978|6|Mentioned|p528 Fig.2.|Late Jurassic|Late Jurassic|||||||
5507|Dingo Claystone|65708|5|Briefly described|p99, 107|Late Jurassic|Late Jurassic|The most significant source rock on the North West Shelf. Accumulated in restricted marine depocentres. Moderate quality source potential, overall gas-prone; more oil-prone intervals in the Oxfordian-Kimmeridgian. Occurs as Dingo Shale on p99.|||||Mudrocks, shale.|29-JUN-22
5507|Dingo Claystone|66126|6|Mentioned|p206|Late Jurassic|Middle Jurassic|Carnarvon Basin.||||||
5507|Dingo Claystone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey claystone/siltstone with thin stringers of light grey siltstone/sandstone - lenticular bedding.|
5507|Dingo Claystone|67200|5|Briefly described|p8 fig 6, p48, p54, p64, app 2 p6|Jurassic|Jurassic|Thermal conductivity of 1.15 W/mK||||Overlies Athol Formation|Siltstone and claystone with thin stringers of siltstone/sandstone - lenticular bedding.|
5507|Dingo Claystone|67368|6|Mentioned|p209 Fig.4.|Late Jurassic|Late Jurassic|Source rock.||||Unconformably overlies Legendre and Eliassen Formations. Is overlain by Angel Formation.||
5507|Dingo Claystone|67970|5|Briefly described|p3, p5, p9, pp13-14, p25 Fig.4.|Kimmeridgian|Oxfordian|Rocks equivalent to this unit were deposited in rifted troughs: the Exmouth, Barrow and Dampier Sub-basins. Targeted for oil, but revealed significant gas shows. Equivalent units provide a top seal to Triassic reservoirs.||||Overlies Jansz Sandstone.||
5507|Dingo Claystone|68135|6|Mentioned|p51, p64|Early Cretaceous|Late Jurassic|Northern Carnarvon Basin. Deposition in restricted marine environment.||||||14-SEP-17
5507|Dingo Claystone|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13|Jurassic|Jurassic |Carnarvon Basin. See also Ch3 p23-26, Ch3 p35, Ch3 p53, Ch3 p65-p66, Ch3 p73. ||||||
5507|Dingo Claystone|69689|6|Mentioned|p16|Jurassic|Jurassic|Exmouth, Dampier, Beagle Sub-basins, Exmouth Plateau, Northern Carnarvon Basin. Part of regional play interval J50.||||Overlies Angel Formation. Is overlain by Forestier Claystone.||05-APR-22
5507|Dingo Claystone|70066|5|Briefly described|Dampier: Fig.2; p1-4. Exmouth: Fig.2; p3|Tithonian|Callovian|See also Regional: Fig.6; p5, p8-9. Northern Carnarvon Basin. The principal oil-prone source rock in the Barrow, Dampier and Exmouth Sub-basins. Potential intraformational seals.||||Overlies Calypso or Eliassen Formations. Is overlain by Angel Formation or Forestier Claystone.|Includes condensed marls and claystones.|
5507|Dingo Claystone|70906|5|Briefly described|p757-758|Jurassic|Jurassic|Gorgon Platform.||||Overlies Athol Formation. Is overlain by Barrow Group.||
5507|Dingo Claystone|73564|5|Briefly described|p1223, 1225|Jurassic|Jurassic|Exmouth Plateau, Gascoyne Margin.||||Overlies Athol Formation. Is overlain by Barrow Group.|Shallow- to deep-marine clastic sediments.|
5517|Diorite Bore Metamorphic Complex|37213|4|Described|p11|||||||||
5517|Diorite Bore Metamorphic Complex|40937|5|Briefly described|p18|||||||||
5540|Djada Hill Lamproite|41158|6|Mentioned|Table 52|||Previous spelling has been Dadja Hill||||||
5578|Domal Porphyry|30766|6|Mentioned|p16|||||||||
5600|Dongara Sandstone|12758|5|Briefly described|p11, p12 Fig. 11|Late Permian|Late Permian|Northern Geological Province:  Perth Basin.||||||
5600|Dongara Sandstone|14227|5|Briefly described|p7, p10|Midian|Kungarian|Shallow marine deposits. See also Enclosure 2.||||||07-FEB-11
5600|Dongara Sandstone|23172|4|Described|Map Legend|Late Permian|Late Permian|||||||
5600|Dongara Sandstone|23279|4|Described|p15-8|Late Permian|Kungurian|(Playford et al., 1976).||||||
5600|Dongara Sandstone|23360|5|Briefly described|846 Fig.1|Permian|Permian|||||||
5600|Dongara Sandstone|23520|5|Briefly described|p11 Fig. 7|Late Permian|Late Permian|Geological Province: Perth Basin. See also p28.||||||22-JUL-09
5600|Dongara Sandstone|24390|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin. See also p13-14.||||||22-JUL-09
5600|Dongara Sandstone|24443|5|Briefly described|Fig.30|Early Triassic|Late Permian|Unconformably overlies Carynginia Formation. Conformably overlain by Kockatea Shale. Geological Province: Bight Basin.||||||10-JAN-05
5600|Dongara Sandstone|31561|6|Mentioned|p18|||Stratigraphic column||||||
5600|Dongara Sandstone|35282|6|Mentioned|Fig.2|||||||||
5600|Dongara Sandstone|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
5600|Dongara Sandstone|36911|6|Mentioned|p57|||||||||
5600|Dongara Sandstone|38352|6|Mentioned|p61|||||||||
5600|Dongara Sandstone|38486|6|Mentioned|p7|||||||||
5600|Dongara Sandstone|41172|6|Mentioned|p124|||||||||
5600|Dongara Sandstone|41195|6|Mentioned|p321|||||||||
5600|Dongara Sandstone|43296|5|Briefly described|Map Legend||Permian|||||||
5600|Dongara Sandstone|43495|4|Described|6-32||Kazanian|||||||
5600|Dongara Sandstone|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
5600|Dongara Sandstone|50620|5|Briefly described|p200 Fig. 8|Late Permian|Late Permian|Geological Province: Perth Basin.||||||
5600|Dongara Sandstone|60376|5|Briefly described|p17 Fig. 4.|Late Permian|Late Permian|Geological Province: Perth Basin. Unconformable contacts either side of the unit.||||||07-FEB-11
5600|Dongara Sandstone|60377|5|Briefly described|p61 Fig. 3|Wuchiapingian|Capitanian|Overlain by Bookara Sandstone Member and the Hovea Member of the Kockatea Shale. Underlain by Wagina Formation. Geological Province: Perth Basin. Foreshore Marine depositional environment.||||||07-FEB-11
5600|Dongara Sandstone|60386|5|Briefly described|p297, 304, 313|Lopingian|Guadalupian|Northern Perth Basin. Massive shallow marine sands. Age shown as ~Late Permian.?Includes volcanics dated at 261-267 +/-5 Ma.||||Overlies Carynginia Formation. Coeval with Beekeeper Formation.||
5600|Dongara Sandstone|60420|5|Briefly described|p424, 425 Fig. 2|Late Permian|Late Permian|Capped by the impermeable Hovea Member (Kockatea Shale). Sandstone.||||||27-SEP-07
5600|Dongara Sandstone|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||10-APR-08
5600|Dongara Sandstone|61546|5|Briefly described|p381, p382, p385 Fig.5.|Early Triassic|Late Permian|Perth Basin. Part of the commercially viable Cliff Head oil field. Excellent reservoir characteristics, with porosities around 20%.||||Overlies Wagina Formation. Is overlain by Kockatea Shale.||
5600|Dongara Sandstone|61811|5|Briefly described|p3 Fig.2, p39, p63.|Late Permian|Middle Permian|Northern Perth Basin. Lateral equivalent of Wagina Sandstone to the north and of Beekeeper Formation to the south. Type section details in Appendix 1.||||Is unconformably overlain by Kockatea Shale.|Shoreface sandstone.|
5600|Dongara Sandstone|64099|5|Briefly described|p368, 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.||||||
5600|Dongara Sandstone|64635|5|Briefly described|p4 Fig.3, p23  |Wuchiapingian|Kungurian|||||Coeval with the Wagina Sandstone and Beekeeper Formation.||
5600|Dongara Sandstone|64972|6|Mentioned|p617 Fig. 5|Late Permian|Late Permian|Geological Province: Perth Basin.||||||
5600|Dongara Sandstone|64980|5|Briefly described|pp625-634.|Early Triassic|Permian|Perth Basin. Shallow marine environment, possibly as fan-delta complex or proximal fan. Hydrocarbon reservoir; its properties and field history are detailed in the article.|||||Massive, predominantly medium to coarse-grained, moderately to well sorted, quartzose sandstone; heavy mineral concentrations and shaly intercalations in the middle part; fine to coarse quartz sandstone in lower parts.|
5600|Dongara Sandstone|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin. Lateral equivalent of Wagina Sandstone to the north, and Beekeeper Formation to the south.||||Is overlain by Kockatea Shale.||
5600|Dongara Sandstone|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
5600|Dongara Sandstone|67370|6|Mentioned|p315.|Late Permian|Late Permian|||||||
5600|Dongara Sandstone|69029|6|Mentioned|p332|Permian|Permian|Of Perth Basin.||||Overlain by Beekeeper Formation. Underlain by Wagina Sandstone.||
5600|Dongara Sandstone|69081|6|Mentioned|p735|Permian|Permian|oil and gas produced. Age: upper Permian. Geol. Prov: Perth Basin||||||
5600|Dongara Sandstone|69182|4|Described|Ch2 p9, Ch2 p12, Ch2 p34-p41|Late Permian|Late Permian|Perth Basin. Deposited either on a shoreline or shoreface. Potentially significant reservoir for the storage of carbon dioxide as its porosity is generally between 10 and 25 percent and permeability is often in the hundreds of mD. Up to 336m thick but generally below 60m thick. See also Ch2 p44-p49, Ch2 p54-p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p80, Ch2 p83-p84, Ch2 p88-p96, Ch2 p98, Ch2 p100, Ch2 p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110-p112.||||Unconformably overlain by the Kockatea Shale. Equivalent to the Wagina Sandstone and Beekeeper Formation.|Massive, medium to well-sorted, coarse grained sandstone.|
5600|Dongara Sandstone|69297|6|Mentioned|p202, p237|||Perth Basin. ||||||
5600|Dongara Sandstone|70097|5|Briefly described|p2, p9, p20 Fig.4, p22 Fig.6|Wuchiapingian|Wuchiapingian|North Perth Basin, a second phase of proximal fan to coarse-grained deltaic deposition. Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough. In Fig.4: age at Dandaragan Trough is Wuchiapingian; and, undifferentiated Dongara and Wagina Sandstones at Greenough/Bookara Shelf and Dongara Saddle are Wordian - late Wuchiapingian. See also Dongara Sandstone Member in this paper.||||Overlies Wagina Sandstone, Beekeeper or Carynginia Formations. Is overlain by Wittecarra Sandstone or Kockatea Shale.|Sandstone.|12-SEP-17
5600|Dongara Sandstone|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Carynginia Formation. Is overlain unconformably by Kockatea Shale.||
5600|Dongara Sandstone|70774|5|Briefly described|p5 fig 3|Dorashamian|Kazanian|Northern Perth Basin.||||Equivalent to the Beekeeper Formation and the Wagina Sandstone.||
5600|Dongara Sandstone|71146|5|Briefly described|p6,  p43 fig 33, p44|Lopingian|Guadalupian|Perth Basin.||||Overlies the Beekeeper Formation. Overlain by the Kockatea Shale.|Sandstone.|
5600|Dongara Sandstone|72258|5|Briefly described|p129,133,135|Lopingian|Guadalupian|Of Perth Basin. Neoarchean (2800-2600 Ma) detrital zircons attributed to Yilgarn Craton, along eastern boundary of Perth Basin (Kositcin et al., 2008; Mole et al., 2013; Nemchin and Pidgeon, 1997). Older material (3700-3000 Ma) probably also derived from Yilgarn Craton. Major peak in Mesoproterozoic (1300-1100 Ma) and minor Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen. Bimodal Neoproterozoic 750 and 500 Ma peaks in detrital zircon ages also likely to be derived locally from Pinjarra Orogen (p134-135 describes potential, but unlikely Gondwanan sources).||||Laterally gradees into Willespie Formation.||
5600|Dongara Sandstone|72505|5|Briefly described|p890|Changhsingian|Wordian|Perth Basin. Correlates with Didecriletes ericanus and Dulhuntyispora parvithola zones.||||Interfingers with and overlies the Beekeeper Formation. Intefingered with the Wagina Sandstone. Overlain by the Kockatea Shale.||18-MAR-20
5600|Dongara Sandstone|72910|6|Mentioned|p4 Fig.3.|Late Permian|Late Permian|Shown as part of the Northern Perth Basin.||||Underlies Kockatea Shale. Shown as laterally equivalent to Wagina Sandstone and Beekeeper Formation.||
5600|Dongara Sandstone|73304|6|Mentioned|p77|||||||||
5600|Dongara Sandstone|73513|5|Briefly described|p30 Fig.2, p32-33|Tatarian|Kazanian|Perth Basin. Deposited in shoreface settings. Misspelt as Dongara Formation p35 Fig.7, p39.||||Overlies Wagina Sandstone, underlies Kockatea Shale|Sandstone.|
5615|Doodlakine Granite|38539|6|Mentioned|Fig.5|||||||||
5618|Doolgunna Formation|7161|5|Briefly described|p92, p92 Fig.4, p93, p97|||Neds Creek Basin. Less than 1900m thick (from p92 Fig.4).||||Overlain by the Karalundi Formation.|Mud-prone rhythmites, laminites, and organic-rich shale (base); debris flow deposits in distributary channels (middle); and mud-stone and  mudrock (top).|
5618|Doolgunna Formation|12099|4|Described|p677-680,  Figs.2, 4, Fig.5, p683|Paleoproterozoic|Paleoproterozoic|Placed in Glengarry Group by Gee (1987) and Gee and Grey (1993). Accumulated in a high energy graben setting (Pirajno, 1996). Rift-fill facies. Distribution is centred around the Goodin Inlier in a broad northeast-trending belt. Possibly sourced from Archean rocks of the Goodin and Marymia Inliers. Intruded by tholeiitic sills.||Unit in Mooloogool Subgroup.||In fault contact with Karalundi Formation in the southeast and east of the Bryah Basin. Interdigitates with mafic volcanics of the Killara Formation.|Contains conglomerate, turbidite rocks and megabreccia units.|04-MAR-13
5618|Doolgunna Formation|22493|6|Mentioned|p93|||||||||
5618|Doolgunna Formation|22940|4|Described|Fig.1 p3|||See also Table 2 p12. of Mooloogool Subgroup, Yerrida Group.||||||
5618|Doolgunna Formation|23589|5|Briefly described|p18|||Of Mooloogool Subgroup.||||||
5618|Doolgunna Formation|23593|4|Described|p11|||Overlying unit Killara Formation. Underlying unit Thaduna Formation. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|23597|5|Briefly described|p2 Fig 1|||Of Yerrida Group. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|23600|4|Described|p10|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Overlying unit Killara Formation. Underlying unit Thaduna Formation. Geological Province: Yerrida Basin. Max. thickness: 2000 m.||||||
5618|Doolgunna Formation|23744|5|Briefly described|p2 Fig 1|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
5618|Doolgunna Formation|23747|4|Described|p6|Paleoproterozoic|Paleoproterozoic|See also page 4 table 1. Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
5618|Doolgunna Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|23749|4|Described|p8|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|23865|5|Briefly described|p170|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
5618|Doolgunna Formation|23890|5|Briefly described|p21 Fig.11|||Of Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|24021|3|Fully described|p3|Paleoproterozoic|Paleoproterozoic|Parent: Mooloogool Subgroup. Geological Province: Yerrida Basin.||||||20-JAN-10
5618|Doolgunna Formation|24028|5|Briefly described|p288|Paleoproterozoic|Paleoproterozoic|Of Mooloogool Subgroup.  Geological Province: Yerrida Basin.||||||07-NOV-08
5618|Doolgunna Formation|24535|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|Rift fill conglomerates, megabreccias and turbidites. Of the Mooloogool Group. Geological Province: Yerrida Basin.||||Interdigitates with Thaduna  Formation and Killara Formation.||26-NOV-13
5618|Doolgunna Formation|40297|6|Mentioned|Fig.1|||||||||
5618|Doolgunna Formation|40937|6|Mentioned|p28|||||||||
5618|Doolgunna Formation|40938|6|Mentioned|p11|||Mention Fig.5||||||
5618|Doolgunna Formation|40989|4|Described|p17|||||||||
5618|Doolgunna Formation|43069|5|Briefly described|p18|||of Glengarry Group||||||
5618|Doolgunna Formation|43238|5|Briefly described|p6|||||||||
5618|Doolgunna Formation|43836|5|Briefly described|Map Legend||Proterozoic|||||||
5618|Doolgunna Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group).  Arkosic sandstone and quartz siltstone; minor pebble beds.||||||18-MAY-04
5618|Doolgunna Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
5618|Doolgunna Formation|49893|5|Briefly described|p2 Fig.1|Proterozoic|Proterozoic|Of the Mooloogool Subgroup (Yerrida Group). Geological Province: Yerrida Basin.||||||
5618|Doolgunna Formation|49896|5|Briefly described|p3 Tb. 2|||Of the Mooloogool Subgroup (Yerrida Group). ||||||
5618|Doolgunna Formation|50222|4|Described|p320 Fig. 3, p322|Paleoproterozoic|Paleoproterozoic|Of the Mooloogool Group.  Conglomerates, arkosic turbidite rocks and megabreccia units. Interdigitates with Thaduna and Killara Formations.   Geological Province: Yerrida Basin.  See also p319 Fig. 2.||||||09-DEC-08
5618|Doolgunna Formation|50226|5|Briefly described|p420, p421 Fig. 4|||Of the Mooloogool Group.  Geological Province: Yerrida Basin.||||||24-JUN-04
5618|Doolgunna Formation|61271|6|Mentioned|p105 Fig.1|||Of the Mooloogool Subgroup.||||||
5618|Doolgunna Formation|62289|4|Described|plate 1, p3-4, p7 Fig. 3, p12-14, p17|Palaeoproterozoic|Palaeoproterozoic|Supersedes Doolgunna Arkose of Gee (1979); of Mooloogool Subgroup; overlain probably unconformably by Maraloou Formation; interdigitates with Killara and Thaduna Formations; arkosic sandstone and quartz wacke.||||||
5618|Doolgunna Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Geol. Prov: Yerrida Basin.||Of Mooloogool Subgroup, Yerrida Group.||Coeval and interbedded with Killara and Thaduna Formations. Overlies Johnson Cairn Formation.|Arkosic sandstone, minor subarkosic to quartzose sandstone, granule conglomerate, and shale.|14-APR-11
5618|Doolgunna Formation|63866|5|Briefly described|p165|||Yerrida Basin. Several kilometres thick.||Mooloogool Subgroup|||Sandstone.|
5618|Doolgunna Formation|64384|5|Briefly described|p78 Tb. 8|||Of the Glengarry Group. Geological province: Glengarry Sub-basin. Granite-derived turbidites of sandstone, arkose.||||||07-FEB-11
5618|Doolgunna Formation|64580|4|Described|map legend||Paleoproterozoic|Of Mooloogool Group. Diamictite and polymictic conglomerate with arkosic matrix; Arkosic sandstone and quartz wacke; minor conglomerate; quartz siltstone; and laminated quartz sandstone.||||||09-DEC-08
5618|Doolgunna Formation|65408|4|Described|pp82-83, p84 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Mooloogool Subgroup.||Intercalated with Killara Formation lavas and sills.|Dominantly turbiditic; arkosic sandstone, siltstone, shale, quartz wacke.|
5618|Doolgunna Formation|65411|6|Mentioned|p89 Fig.1.|||||Unit in Mooloogool Subgroup.||||
5618|Doolgunna Formation|65412|6|Mentioned|p101 Fig.4.|||||||||
5618|Doolgunna Formation|65419|1|Redefined|p3, p4 Fig.1, p18, p19, p25, p49.|Paleoproterozoic|Paleoproterozoic|Has type area but no type section has been selected yet. Incorporates strata referred to as Doolgunna Arkose by Gee (1979) and Elias et al. (1982);  modified to Doolgunna Formation by Gee (1987) after recognising its heterolithic nature; further revised in this study. Some areas previously mapped as this unit on southeast Peak Hill 1:250 000 sheet are now placed in the Thaduna Formation. This unit also excludes strata now assigned to the Peak Hill Schist. Named after Doolgunna Homestead.  Thickness uncertain; up to a few kms.||Unit in Mooloogool Subgroup.||Disconformably overlies and interfingers with Johnson Cairn Formation. Is faulted against the Karalundi Formation. Is unconformably overlain by Mount Leake Formation.|Arenaceous to silty arkose and quartz wacke, with subrounded to subangular grains, mainly unsorted; many beds contain intraclasts; conglomeratic bands and pebble beds are commonly interbedded; includes diamictite with very large angular blocks.|15-NOV-13
5618|Doolgunna Formation|65472|5|Briefly described|p2, p3 Fig.2|||Yerrida Basin.||Mooloogool Group|||with Thaduna Formation, conglomerate and turbidite facies|
5618|Doolgunna Formation|65913|4|Described|p2 Fig.1, p6. |Paleoproterozoic|Paleoproterozoic|Includes cyclic units, fining-upwards with broad concave bases suggesting channelised turbidity flow possibly in a mid-fan setting. Main direction of transport was to the east.||Unit in Mooloogool Subgroup.||Overlies Johnson Cairn Formation. Is intercalated with Killara Formation. Is overlain by Maraloou Formation and, unconformably, by Earaheedy Group.|Diamictite, ferruginised  arkosic sandstone with argillaceous rip-up clasts, siltstone, shale; iron content increases higher in the succession.|
5618|Doolgunna Formation|66427|6|Mentioned|p72 Fig.26, |||Deposition of immature sediments from orogenic highlands.||||||
5618|Doolgunna Formation|68561|5|Briefly described|500K_GEOLOGYP08_LUT.csv||Paleoproterozoic|||Mooloogool Group|||Diamictite and polymictic conglomerate with arkosic matrix; Arkosic sandstone and quartz wacke; minor conglomerate; quartz siltstone; and laminated quartz sandstone|
5618|Doolgunna Formation|69003|5|Briefly described|p11-12|||Yerrida Basin.||Mooloogool Group.||Unconformably overlies Johnson Cairn Formation.||
5618|Doolgunna Formation|69152|4|Described|500k_geologyp08_lut||Paleoproterozoic|||Mooloogool Group|||Arkosic sandstone and quartz wacke; minor conglomerate; quartz siltstone; and laminated quartz sandstone.|05-AUG-15
5618|Doolgunna Formation|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Mooloogool Group|||Arkosic sandstone and quartz wacke; minor conglomerate; quartz siltstone and laminated quartz sandstone. Diamictite and polymictic conglomerate with arkosic matrix.|
5618|Doolgunna Formation|69596|6|Mentioned|p9-10|||Yerrida Basin.||Mooloogool Group.||||
5618|Doolgunna Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||2500 - 1600 Ma (inferred).|Mooloogool Group|||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, and laminated quartz sandstone.|
5618|Doolgunna Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin|2500-1600 Ma||||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone and laminated quartz sandstone.|
5618|Doolgunna Formation|70796|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen. See also glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|ca 25001600 Ma (inferred)|Mooloogool Group|||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, and laminated quartz sandstone.|
5618|Doolgunna Formation|70804|5|Briefly described|p2, p6, p22-p23, p43|||Previously of the Glengarry Group.||Mooloogool Subgroup||Faulted against the Karalundi Formation.||
5618|Doolgunna Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sedimentary breccia, sandstone|
5618|Doolgunna Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, and laminated quartz sandstone|
5618|Doolgunna Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Capricorn Orogeny (1817 - 1772 Ma). See  500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|2170-1600 Ma (inferred)|Unit of Mooloogool Group.|||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, and laminated quartz sandstone|
5618|Doolgunna Formation|71468|4|Described|p24-26|Orosirian|Orosirian|Geological province: Capricorn Orogen, Yilgarn Craton. Of Yerrida Basin. Broadly coeval with Killara Formation.||Unit of Mooloogool Group.||Laterally grades into Killara Formation. Time-equivalent to Thaduna Formation.|Arkosic sandstone, lithic sandstone, quartz wacke, minor conglomerate, siltstone, mudstone and laminated quartz sandstone that locally contain fragments of basaltic scoria.|
5618|Doolgunna Formation|71484|5|Briefly described|p125,128-129,134|||Geological province:  Of Yerrida Basin. Forms a coherent unit which wraps around the Juderina Formation and lies proximal to the Goodin Inlier and Goodin Fault.||Unit of Mooloogool Group.||Overlain by Maraloou Formation. Underlain by Killara Formation.|Arkosic and lithic sandstone and quartz wacke; minor congloemrate, siltstone, mudstone and laminated quartz sandstone, locally containing fragments of basaltic scoria.|30-AUG-19
5618|Doolgunna Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Mooloogool Group|||Arkosic sandstone and quartz wacke; minor conglomerate, quartz siltstone, and laminated quartz sandstone.|
5760|Duerdin Group|14019|4|Described|p19|||Sandstone, conglomerate, siltstone, diamictite. Subdivided into five formations but only undifferentiated diamictite outcrops in LIMBUNYA. Geological Province: Wolfe Creek Basin.  See also p2 Fig. 1, p3 Fig. 2.||||||
5760|Duerdin Group|22496|4|Described|p10|Neoproterozoic|Neoproterozoic|Includes the Moonlight Valley Tillite, Ranford Formation and Redbank Yard Formation.  Correlated with the Kuniandi Group in MOUNT RAMSAY.||||||12-AUG-04
5760|Duerdin Group|22537|6|Mentioned|34|Proterozoic|Proterozoic|||||||
5760|Duerdin Group|22547|4|Described|p28||Neoproterozoic III|Geological province: Wolfe Creek Basin. Age: c. 610 Ma.||||||14-NOV-06
5760|Duerdin Group|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
5760|Duerdin Group|22754|5|Briefly described|p10|Neoproterozoic|Neoproterozoic|||||||
5760|Duerdin Group|22777|5|Briefly described|Map|||In the Wolfe Basin.||||||14-NOV-06
5760|Duerdin Group|23216|6|Mentioned|Fig3p5||Mesoproterozoic|||||||
5760|Duerdin Group|23314|5|Briefly described|332|||||||||
5760|Duerdin Group|23383|5|Briefly described|p20|||Overlain by Albert Edward Group. Correlated with Louisa Downs Group (Coates & Preiss 1980). Plumb prefers correlation with Kuniandi Group.||||||14-NOV-06
5760|Duerdin Group|23599|6|Mentioned|p17|||||||||
5760|Duerdin Group|23621|4|Described|p33|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Overlain by Albert Edward Group. Geological Province: Wolfe Basin.||||||09-AUG-06
5760|Duerdin Group|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Age: c600 Ma. Geological Province: Wolfe Basin.||||||
5760|Duerdin Group|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
5760|Duerdin Group|24122|6|Mentioned|p2 Fig.1|||Geological Province: Wolfe Creek Basin.||||||
5760|Duerdin Group|24173|4|Described|p25, 33|Neoproterozoic III|Neoproterozoic III|Comprises Moonlight Valley Tillite and Ranford Formation. Overlain by Albert Edward Group; underlain Ruby Plains Group. Geological Province: Wolfe Basin. Age: 650-600Ma. Correlates with Kuniandi Group (MOUNT RAMSAY 1:250,000 sheet area).||||||06-APR-05
5760|Duerdin Group|24297|6|Mentioned|p2 Fig.1|||Geological Province: Wolfe Creek Basin.||||||
5760|Duerdin Group|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Siltstone, mudstone, sandstone, greywacke, dolomitic sandstone, dolomite and tillite.   Age: c.610Ma.  Geological Province: Wolfe Creek Basin.||||||
5760|Duerdin Group|28255|4|Described|p69, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Subdivided into five formations/units. Comprises tillite, fluvio-glacial conglomerate and sandstone, and other glacigene rocks. Unconformably overlies Auvergne Group.||||||
5760|Duerdin Group|29813|4|Described|Table 2|||||||||
5760|Duerdin Group|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5760|Duerdin Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
5760|Duerdin Group|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5760|Duerdin Group|30896|6|Mentioned|p18|||Dated 740 m.y. Refers Bofinger(1967)||||||
5760|Duerdin Group|31393|6|Mentioned|Pl.25|||||||||
5760|Duerdin Group|32172|6|Mentioned|p9|||||||||
5760|Duerdin Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5760|Duerdin Group|32660|4|Described|Table 6|||||||||
5760|Duerdin Group|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
5760|Duerdin Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Ranford Formation, Moonlight Valley Tillite, Blackfellow Creek Sandstone, Fargoo Tillite and the Skinner Sandstone.||||||02-DEC-04
5760|Duerdin Group|32701|4|Described|Table 1|||Adelaidean. See also p14.||||||09-AUG-06
5760|Duerdin Group|32728|6|Mentioned|p3|||||||||
5760|Duerdin Group|33375|6|Mentioned|p13, p11 Tb. 1|Adelaidean|Adelaidean|||||||26-APR-05
5760|Duerdin Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5760|Duerdin Group|33377|5|Briefly described|Table 2|||||||||
5760|Duerdin Group|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|||||||27-APR-05
5760|Duerdin Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5760|Duerdin Group|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
5760|Duerdin Group|36551|6|Mentioned|Table 12|||||||||
5760|Duerdin Group|36888|4|Described|p215|||||||||
5760|Duerdin Group|36898|6|Mentioned|p183|||||||||
5760|Duerdin Group|37299|6|Mentioned|Fig.1|||||||||
5760|Duerdin Group|37462|4|Described|Table 4.X|||||||||
5760|Duerdin Group|37927|6|Mentioned|p504|||||||||
5760|Duerdin Group|38157|6|Mentioned|Table X|||||||||
5760|Duerdin Group|38988|6|Mentioned|Fig.4|||||||||
5760|Duerdin Group|39210|5|Briefly described|p49|||||||||
5760|Duerdin Group|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
5760|Duerdin Group|40105|6|Mentioned|p313|||||||||
5760|Duerdin Group|40494|4|Described|p11|||||||||
5760|Duerdin Group|41864|6|Mentioned|p63|||||||||
5760|Duerdin Group|41883|6|Mentioned|p65|||||||||
5760|Duerdin Group|42811|6|Mentioned|p30|||||||||
5760|Duerdin Group|43299|5|Briefly described|Map Legend||Neoproterozoic|||||||
5760|Duerdin Group|43303|5|Briefly described|Map Legend||Neoproterozoic|||||||
5760|Duerdin Group|43595|6|Mentioned|p444,Fig5-34,p551||Neoproterozoic|||||||
5760|Duerdin Group|43853|5|Briefly described|Map Legend||Proterozoic|||||||
5760|Duerdin Group|43855|5|Briefly described|Map Legend||Proterozoic|||||||
5760|Duerdin Group|44140|5|Briefly described|p300, p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. Associated with the 670 Ma Marinoan glaciation.|||Fargoo, Moonlight Valley Tillites; Frank River Sandstone; Ranford Formation.|Is overlain unconformably by Albert Edward Group.||07-MAR-18
5760|Duerdin Group|44155|6|Mentioned|p254 Fig.3-40|Neoproterozoic|Neoproterozoic|Sturt Block, Kimberley region.||||||
5760|Duerdin Group|44230|5|Briefly described|Map Legend||Proterozoic|||||||
5760|Duerdin Group|44317|4|Described|Table 3||Adelaidean|||||||
5760|Duerdin Group|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
5760|Duerdin Group|44324|14|Not recorded|p.10||Adelaidean|Tb.2. (Adelaidean).||||||
5760|Duerdin Group|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
5760|Duerdin Group|44363|4|Described|p.6,14,16,17,21,22||Neoproterozoic|Upper Proterozoic, units.||||||
5760|Duerdin Group|44364|14|Not recorded|map legend|||||||||
5760|Duerdin Group|44366|14|Not recorded|p.17|||||||||
5760|Duerdin Group|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
5760|Duerdin Group|45047|2|Defined|p82|Adelaidean|Adelaidean|See also p36.||||||09-AUG-06
5760|Duerdin Group|45112|6|Mentioned|p12|||||||||
5760|Duerdin Group|45140|2|Defined|p13-14, p40, p59-60, p66, p75|||See also Appx.p33-34. Dow and Gemuts (1969). Named after Duerdin Creek. Kimberley and Victoria River regions, and an unnamed basin NW of Birrindudu Basin. Probably over 500m thick. No fossils known. Folded and faulted.|~700 Ma (Plumb and Derrick, 1975).||Redbank Yard, Ranford Formations.|Unconformably overlies Wade Creek Sandstone, Helicopter Siltstone and Auvergne Group. Is overlain unconformably by Albert Edward Group and (inferred) Carranya Beds.|Includes glacigene rocks.|
5760|Duerdin Group|46864|5|Briefly described|p40|||||||||
5760|Duerdin Group|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
5760|Duerdin Group|48931|6|Mentioned|p59|||Correlation. Refers Dow & Gemuts(1969)||||||
5760|Duerdin Group|48938|4|Described|p60|||||||||
5760|Duerdin Group|48943|3|Fully described|p77|||||||||
5760|Duerdin Group|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Sandstone, conglomerate, siltstone, diamicrite||||||
5760|Duerdin Group|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Wolfe Creek Basin. Includes: Fargoo Tillite, Moonlight Valley Tillite, Ranford Formation.||||||
5760|Duerdin Group|60589|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, conglomerate, siltstone, diamictite.  Geological Province: Wolfe Creek Basin.||||||24-NOV-04
5760|Duerdin Group|60682|5|Briefly described|p17|Neoproterozoic|Neoproterozoic|Contains 7 formations. Geological Province: Wolfe Creek Basin.||||||
5760|Duerdin Group|60685|5|Briefly described|p2 Fig. 1|||Geological Province: Wolfe Creek Basin.||||||
5760|Duerdin Group|60724|6|Mentioned|p5 Fig. 2|||||||||
5760|Duerdin Group|63458|5|Briefly described|p872-874; p884; p886, p897 Figs.11,19. |Ediacaran|Cryogenian|East Kimberley area.|||Includes Fargoo and Moonlight Valley Tillites; Skinner, Frank River, Blackfellow Sandstones; Ranford Formation.|Underlies the Albert Edward Group unconformably.||
5760|Duerdin Group|64104|4|Described|p61-80|Neoproterozoic|Neoproterozoic|Eastern margin of Halls Creek Orogen. Weakly deformed; gently to moderately dipping strata.|||Includes Fargoo, Moonlight Valley, Ranford Formations; Frank River Sandstone.|Overlies Helicopter Siltstone; overlies Olympio Formation unconformably; overlies Eliot Range Formation disconformably. Is overlain unconformably by Albert Edward Group.||
5760|Duerdin Group|64580|4|Described|map legend|Ediacaran|Ediacaran|Siltstone, mudstone, sandstone, greywacke, dolomitic sandstone, dolomite, and tillite.||||||09-DEC-08
5760|Duerdin Group|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Wolfe Basin during the Centralian 3 event (~600-544 Ma)||||||
5760|Duerdin Group|65232|6|Mentioned|p5 Fig. 4|||Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
5760|Duerdin Group|65331|5|Briefly described|Map legend + overview geology map legend|Neoproterozoic |Neoproterozoic |Of Wolfe Creek Basin. Includes Big Knob beds, Ranford Formation, Moonlight Valley Tillite, Blackfellow Creek Sandstone, Fargoo Tillite, Skinner Sandstone, Bullo River Sandstone. Sandstone, conglomerate, siltstone, diamictite, dolostone ||||||
5760|Duerdin Group|65339|6|Mentioned|p5 Fig.4. ||||||||Conglomerate, sandstone, mudstone, diamictite.|
5760|Duerdin Group|65413|6|Mentioned|p104.|||||||Faulted against McHale Granodiorite.||
5760|Duerdin Group|65417|5|Briefly described|p156, p164 Fig.7, p165.|Neoproterozoic|Neoproterozoic|Glacial deposits. A major period of strike-slip faulting occurred after this unit formed and before the Antrim Plateau Volcanics (c.550 Ma).|c.650 Ma.|||Unconformably overlies Carr Boyd Group.||
5760|Duerdin Group|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.|||Includes Skinner and Blackfellow Creek Sandstones; Fargoo and Moonlight Valley Tillites; and Ranford Formation.|Unconformably overlies Auvergne Group. Is unconformably overlain by Kinevans Sandstone.||
5760|Duerdin Group|67484|6|Mentioned|p294, p295 Figs.1,2|Ediacaran|Cryogenian|East Kimberley.|||Fargoo, Moonlight Valley Tillites; Ranford Formation; Frank River Sandstone.|Overlain by Albert Edward Group.||
5760|Duerdin Group|67620|6|Mentioned|p2-3, 5|Ediacaran|Cryogenian||||Fargoo, Moonlight Valley, Ranford Formations; Frank River Sandstone; Jarrad Sandstone Member; Johnny Cake Shale Member.|Is overlain by Albert Edward Group.||
5760|Duerdin Group|68138|6|Mentioned|p153-154, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.|||Fargoo, Moonlight Valley, Ranford Formations; Frank River Sandstone.|||
5760|Duerdin Group|68244|4|Described|p659-660,666-669|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Preserved on the eastern margin of the Halls Creek Orogen, with outcrop extending NE from the WA-NT border near Kununurra to SE of Halls Creek. Gently-folded beneath the Albert Edward Group (not folded).|||Includes Ranford Formation, Moonlight Valley Formation, Frank River Sandstone and Fargoo Formation.|Overlain unconformably by Albert Edward Group.||
5760|Duerdin Group|68473|6|Mentioned|p530-532|Neoproterozoic|Neoproterozoic|Kimberley region.|||Includes the Fargoo Tillite, Frank River Sandstone, Moonlight Valley Tillite, Jarrad Sandstone, Johnny Cake Shale, Ranford Formation.|||
5760|Duerdin Group|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Ediacaran|Ediacaran|Wolfe Creek Basin, Halls Creek Orogen. See also 500k_intergeop_lut.csv|||||Undivided; siltstone, mudstone, sandstone, greywacke, dolomitic sandstone, dolomite and tillite.|
5760|Duerdin Group|68733|5|Briefly described|p171,p181,p183-185, p187-189, p191, p193|Cryogenian|Cryogenian|Youngest Group in the Victoria Basin. Also within the Wolfe Basin.|||Includes Moonlight Valley Tillite, Blackfellow Creek Siltstone, Fargoo Tillite, and Bullo River Sandstone (basal unit).||Includes basal siltstones and sandstones.|05-DEC-17
5760|Duerdin Group|69003|6|Mentioned|p5|||Halls Creek Orogen.||||||
5760|Duerdin Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin|||Includes Ranford Formation, Moonlight Valley Tillite, Frank River Sandstone, Fargoo Tillite, Redbank Yard Formation||Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstone, quartz sandstone, dolomite, and tillite|31-JUL-15
5760|Duerdin Group|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv. |||Includes Ranford Formation, Moonlight Valley Tillite, Frank River Sandstone, Fargoo Tillite, Redbank Yard Formation||Undivided; Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstones, quartz sandstone,  greywacke, dolomitic sandstone, dolomite and tillite.|
5760|Duerdin Group|69422|6|Mentioned|p7:2 Fig.7.2|Neoproterozoic|Neoproterozoic|Wolfe Basin.||||||12-JUL-16
5760|Duerdin Group|69437|5|Briefly described|p22:7|||Wolfe Basin, Centralian A Superbasin. Supersequence 3.|||Skinner, Blackfellow Creek Sandstones; Fargoo, Moonlight Valley Tillites; Ranford Formation.|||12-JUL-16
5760|Duerdin Group|69442|5|Briefly described|p27:1-7|||Dow and Gemuts (1969); Sweet et al. (1974). Dunster et al. (2000) included the previously unassigned Bullo River Sandstone and Big Knob beds. Dunster (this study, 2013) includes Uniya Formation and undifferentiated diamictite in the Wolfe Basin, but not explicitly in the Duerdin Group. All of this Group has been affected by near-vertical NNW-trending faults, some with several hundred metres of sinistral displacement.|||Skinner, Blackfellow Creek, Bullo River Sandstones; Fargoo, Moonlight Valley Tillites; Ranford Formation; Big Knob beds.|||12-JUL-16
5760|Duerdin Group|69587|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen, North Australian Craton. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|635-541 Ma (inferred)||||Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstone, quartz sandstone, dolomite, and tillite|
5760|Duerdin Group|69597|6|Mentioned|p5 fig 2b|||||||||
5760|Duerdin Group|69634|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|635-541 Ma (Inferred)||Includes Fargoo Tillite, Frank River Sandstone, Ranford Formation, Moonlight Valley Tillite, Redbank Yard Formation.||Undivided; siltstone, mudstone, sandstone, greywacke, dolomitic sandstone, dolomite, and tillite|
5760|Duerdin Group|69673|6|Mentioned|p189, p190|Neoproterozoic|Neoproterozoic||||Includes Skinner Sandstone, Fargoo Tillite, Blackfellow Creek Sandstone, Moonlight Valley Tillite, Ranford Formation, Bullo River Sandstone, Big Knob beds|||
5760|Duerdin Group|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian|See also 500k_interpgeop_lut.csv.|541-850 Ma||Includes Ranford Formation, Moonlight Valley Tillite, Frank River Sandstone, Fargoo Tillite, Redbank Yard Formation||Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstone, quartz sandstone, dolomite, and tillite|
5760|Duerdin Group|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. |||Includes Big Knob beds, Ernie Lagoon, Beasly Knob, Bucket Spring & Jarrad Sandstone Members, Moonlight Valley & Fargoo Tillites, Blackfellow Creek Sandstone, Skinner Sandstone, Bullo River Sandstone|||
5760|Duerdin Group|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.|||Includes Ranford Formation, Moonlight Valley Tillite, Blackfellow Creek Sandstone, Fargoo Tillite, Skinner Sandstone.|Unconformably overlies Auvergne Group. Is unconformably overlain by Kinevans Sandstone, Antrim Plateau Volcanics.||
5760|Duerdin Group|70731|6|Mentioned|p268,278|Neoproterozoic|Neoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||||||
5760|Duerdin Group|70826|6|Mentioned|p5 tbl 2|||Supersequence 3, Centralian Superbasin.||||||20-APR-20
5760|Duerdin Group|70851|5|Briefly described|p6, p17-p19, p29|||Eastern Zone, Lamboo Province.||||Overlies the Bastion Group. Overlain by the Antrim Plateau Volcanics.||
5760|Duerdin Group|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|720-541 Ma (inferred)||Includes Fargoo Tillite, Redbank Yard Formation and Frank River Sandstone.||Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstone, quartz sandstone, dolomite, and tillite|
5760|Duerdin Group|71302|5|Briefly described|p6,73-75|Neoproterozoic|Neoproterozoic|Of Wolfe Basin. Major zircon provenance peaks at c. 1530-1600 Ma (maxima c. 1590 Ma) and c. 1050-1220 Ma coincide with Musgrave province magmatic events.|||Includes Black Point Sandstone Member.|Underlain unconformably by Auvergne Group.||
5760|Duerdin Group|72034|5|Briefly described|500k_interpgeop16_lut|Ediacaran|Cryogenian|Wolfe Basin.|||||Polymictic conglomerate, siltstone, mudstone, lithic and feldspathic sandstone, quartz sandstone, dolomite, and tillite.|
5760|Duerdin Group|73255|6|Mentioned|p533 Fig.1, p534 Fig.2|Ediacaran|Cryogenian|Contains Palaeopaschichnus and Yangtziramulus zhangi vendobiont fossils.|||Fargoo Tillite, Frank River Sandstone, Moonlight Valley Tillite, Ranford Formation.|Overlies the Osmond Range Succession and Helicopter Siltstone, underlies the Albert Edward Group.||
5770|Duffer Formation|22449|6|Mentioned|Table3 P27||Archean|Age of unit is 3460 Ma||||||07-NOV-08
5770|Duffer Formation|22615|6|Mentioned|p 6|||||||||
5770|Duffer Formation|22715|5|Briefly described|table7 p214,216|Archean|Archean|Age: 3520-3400Ma on Table, 3465Ma in taxt||||||07-NOV-08
5770|Duffer Formation|22717|6|Mentioned|P6||Archean|Age of unit is 3500 to 3453+/-16 Ma||||||07-NOV-08
5770|Duffer Formation|23046|5|Briefly described|169|||||||||
5770|Duffer Formation|23206|6|Mentioned|Fig.1|||of Warrawoona Fm.||||||
5770|Duffer Formation|23255|5|Briefly described|p46, 47, Fig.2||Archean|Age: U-Pb single zircon age of 3470+/-3Ma.||||||07-NOV-08
5770|Duffer Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Warrawoona Group, Pilbara Craton||||||07-NOV-08
5770|Duffer Formation|23570|6|Mentioned|p233 Appendix 1|||Supersedes Duffers Creek Porphyry.||||||
5770|Duffer Formation|23755|4|Described|p20|Archean|Archean|See also page 17 table 1. Of Warrawoona Group.||||||07-NOV-08
5770|Duffer Formation|23780|4|Described|p140|Archean|Archean|Age: ~3427+/-2 Ma. Of the Warrawoona Group. Underlain by Mount Ada Basalt.||||||07-NOV-08
5770|Duffer Formation|23783|5|Briefly described|p7 Fig. 2|||Of Talga Talga Subgroup.||||||
5770|Duffer Formation|23784|5|Briefly described|p76|Archean|Archean|Age: 3465 +/- 3Ma.||||||07-NOV-08
5770|Duffer Formation|23807|5|Briefly described|p110|Archean|Archean|Age: 3470-3450Ma (SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|23813|5|Briefly described|p103|Archean|Archean|Age: 3470Ma.  Geological Province: Pilbara Craton.  See also p91 Tb. 1||||||07-NOV-08
5770|Duffer Formation|23895|5|Briefly described|p885 Fig.2, p904|||Of Warrawoona Group.  Overlies the Talga Talga Subgroup.  Geological Province: Pilbara Craton.||||||07-MAR-05
5770|Duffer Formation|23936|5|Briefly described|p16|Archean|Archean|Geological Province: Pilbara Craton. Age: 3470 Ma.||||||07-NOV-08
5770|Duffer Formation|24025|4|Described|p9 Tb. 1|Archean|Archean|Of Talga Talga Subgroup.  Dacitic tuff, lava, and agglomerate, with subordinate rhyolite, basalt, and chert.  Max. Thickness: 8000m.  Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Warrawoona Group. Geological Province: Pilbara Craton||||||07-NOV-08
5770|Duffer Formation|24182|4|Described|p92|||Of the Warrawoona Group. Overlies: Talga Talga Subgroup. Calc-alkaline volcanics. Age: ca.3470 Ma. Geological Province: Pilbara Craton.||||||05-SEP-14
5770|Duffer Formation|24184|4|Described|p699 Fig.3, p700, p701+B66|Archean|Archean|Of the Talga Talga Subgroup. Geological Province: Pilbara Craton. Max Thickness: 5km. Age: ca.3470Ma. Formerly of the Warrawoona Group (Hickman 1990), now included in the Talga Talga Subgroup||||||07-NOV-08
5770|Duffer Formation|24185|5|Briefly described|p734, p742 Tb.4|Archean|Archean|Age: ca. 3471-3463 Ma (Nijman at al, 1998; Van Kranendonk and Morant, 1998). Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|24194|5|Briefly described|p905|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
5770|Duffer Formation|24531|5|Briefly described|p5|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group).  Age: 3474-3463Ma.    Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|24550|5|Briefly described|p31 Tb. 3.1|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Dacitic tuff, agglomerate. Age: 3471-3463. Max. thickness: 5km. Geological Province: Pilbara Craton.||||||07-FEB-11
5770|Duffer Formation|24590|5|Briefly described|p29, p30 Fig. 1.3|Archean|Archean|Of Warrawoona Group; proposed to be grouped within the Talga Talga Subgroup Van Kronendonk 2002). Comprises dacites, dacitic tuff, andesite, volcanoclastic + clastic sedimentary rocks; agglomerates + lava.  Age: 3470-3450Ma. Max. thick: 5km. See also p31.||||||07-FEB-11
5770|Duffer Formation|31309|6|Mentioned|Table 8|||refs Lipple 1975||||||
5770|Duffer Formation|31853|2|Defined|p60|Archean|Archean|||||||07-NOV-08
5770|Duffer Formation|34731|6|Mentioned|p808|||||||||
5770|Duffer Formation|35142|6|Mentioned|p421|||||||||
5770|Duffer Formation|35531|6|Mentioned|Fig.1|||Composite lithostratigraphic section||||||
5770|Duffer Formation|35681|6|Mentioned|Fig.3|||See also Table 2&3.||||||
5770|Duffer Formation|35726|6|Mentioned|p120|||||||||
5770|Duffer Formation|36123|6|Mentioned|p443|||||||||
5770|Duffer Formation|36124|6|Mentioned|p441|||||||||
5770|Duffer Formation|37373|5|Briefly described|p79|||||||||
5770|Duffer Formation|37899|6|Mentioned|Fig.2|||||||||
5770|Duffer Formation|38242|6|Mentioned|p199|||||||||
5770|Duffer Formation|38481|5|Briefly described|p265|||||||||
5770|Duffer Formation|38498|5|Briefly described|Table 1|||||||||
5770|Duffer Formation|38510|6|Mentioned|p188|||||||||
5770|Duffer Formation|38514|5|Briefly described|Table II|||||||||
5770|Duffer Formation|38544|6|Mentioned|Fig.1|||||||||
5770|Duffer Formation|38624|6|Mentioned|p241|||||||||
5770|Duffer Formation|38742|6|Mentioned|p354|||||||||
5770|Duffer Formation|38763|6|Mentioned|p103|||||||||
5770|Duffer Formation|39310|6|Mentioned|p27|||||||||
5770|Duffer Formation|39426|6|Mentioned|Fig.3|||||||||
5770|Duffer Formation|39444|6|Mentioned|Table 1|||||||||
5770|Duffer Formation|39559|6|Mentioned|Table 1|||||||||
5770|Duffer Formation|39672|6|Mentioned|p239|||||||||
5770|Duffer Formation|39697|3|Fully described|p91|||||||||
5770|Duffer Formation|40596|6|Mentioned|p65|||||||||
5770|Duffer Formation|40933|4|Described|p2|||||||||
5770|Duffer Formation|41028|6|Mentioned|p227|||||||||
5770|Duffer Formation|41029|5|Briefly described|p106|||||||||
5770|Duffer Formation|41066|5|Briefly described|1 of 2 FO1|||||||||
5770|Duffer Formation|41252|6|Mentioned|p53|||||||||
5770|Duffer Formation|41350|6|Mentioned|p27|||||||||
5770|Duffer Formation|41624|6|Mentioned|p43|||||||||
5770|Duffer Formation|41636|6|Mentioned|p79|||||||||
5770|Duffer Formation|41767|4|Described|p45|||||||||
5770|Duffer Formation|41851|5|Briefly described|p823|||||||||
5770|Duffer Formation|41892|6|Mentioned|p315|||||||||
5770|Duffer Formation|42231|5|Briefly described|p330|||||||||
5770|Duffer Formation|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
5770|Duffer Formation|43595|5|Briefly described|p213|||||||||
5770|Duffer Formation|43698|6|Mentioned|p26|||||||||
5770|Duffer Formation|43769|5|Briefly described|p858|||3.46 Ga||||||
5770|Duffer Formation|44150|4|Described|p129, p132-133, p138, p140 Tb.2-19|||See also p152 Tb.2-22, p155, p157 Fig.2-144. 5km thick. Formerly part of Friendly Creek Formation (of Fitton et al., 1975) and part of Sharks Formation (Ingram, 1977). Host to most of the Pilbara copper deposits; other mineral deposits occur.|3453 +/- 16 Ma (Zircon U-Pb; Pidgeon, 1978).|Warrawoona Group||Overlies Mount Ada Basalt, partly unconformably.|Metamorphosed (to greenschist) dacite lava, tuff, agglomerate, subordinate rhyolite, basalt and chert; minor porphyritic intrusions.|
5770|Duffer Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Warrawoona Group.  Dacitic, rhyodacitic and andesitic lava, tuff, and agglomerate.  Age: c.3471Ma.||||||07-NOV-08
5770|Duffer Formation|46319|5|Briefly described|p6 Fig. 3|Archean|Archean|Of Warrawoona Group.  Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|50189|4|Described|p9|Archean|Archean|Of the Warrawoona Group. Metamorphosed felsic volcanic rocks with subordinate fine-grained amphibolite. Disconformably overlain by Apex Basalt. Age: 3471 +/- 5Ma. Max. Thickness: 3500m. Intruded by Coppin Gap Granodiorite.||||||27-JAN-17
5770|Duffer Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Talga Talga Subgroup (Warrawoona Group) Geological Province: Pilbara Craton. Age: c. 3470 Ma||||||07-NOV-08
5770|Duffer Formation|50423|5|Briefly described|p215 Fig.1||Archean|3469 Ma.||||||07-NOV-08
5770|Duffer Formation|50427|4|Described|p185, Fig.7, p192 Fig.11|Archean|Archean|Age: 3463-3471 Ma. Of lower Warrawoona Group. Felsic volcanics, shale and tuff.||||||07-NOV-08
5770|Duffer Formation|50430|4|Described|p160||Archean|3470-3463 Ma. Calc-alkaline volcanic complex. In East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
5770|Duffer Formation|50544|3|Fully described|p22, p21 Tb. 4|Archean|Archean|Proposed that it becomes part of the Talga Talga Subgroup. Overlies Mount  Ada Basalt; underlies Apex Basalt. Intruded by Coppin Gap Granodiorite. Max. thickness: ~3500m. Age: 3471+/-5Ma.||||||05-SEP-14
5770|Duffer Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Talga Talga Subgroup (Warrawoona Group). Dacitic, rhyodacitic and andesitic lava, tuff, and agglomerate.  Geological Province: Pilbara Craton.||||||23-DEC-09
5770|Duffer Formation|60112|5|Briefly described|p107 Fig.1, p108.|||||||Overlies Dresser Formation and Mount Ada Basalt. Overlain by the Apex Basalt.|Thin volcaniclastic chert.|
5770|Duffer Formation|60429|4|Described|p7, p9|Archean|Archean|Of the Warrawoona Group. Disconformable on Mount Ada Basalt; overlain disconformably by Apex Basalt. Age: 3470+/-2Ma and 3471+/-5Ma (zircon U-Pb). Max. thickness: 3500m. Composed of metamorphosed felsic voclanic rocks. See also p8 Fig. 4.||||||07-FEB-11
5770|Duffer Formation|60636|5|Briefly described|p10, p46, p50|Archean|Archean|Of the Warrawoona Gp. Massive quartz and plagioclase porphyry rocks predominate. Overlain by Apex Formation; overlies Mount Ada Basalt. Age: ~3466Ma. Geological Province: Pilbara Craton. See also p35-36 Fig. 3.2.||||||07-FEB-11
5770|Duffer Formation|61111|6|Mentioned|p96 Fig.2|||||||||
5770|Duffer Formation|61253|5|Briefly described|p52 Fig. 2|Archean|Archean|Geological Province: eastern Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|61257|5|Briefly described|p355 Tb. 1|Archean|Archean|Metamorphosed felsic volcanics.  Geological Province: North Pole Dome of the Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|61266|4|Described|p58 Tb.1|Archean|Archean|Of the Warrawoona Group. Age: 3471-3463 (McNaughton et al., 1993; Thorpe et al., 1992). Dacitic tuff, agglomerate and lava. Geological Province: Pilbara Craton.||||||07-NOV-08
5770|Duffer Formation|61579|5|Briefly described|p58 Fig. 2|Archean|Archean|Of the Warrawoona Group. Age: 3471-3463Ma. ||||||07-NOV-08
5770|Duffer Formation|62427|5|Briefly described|p2 Fig.1, p3 Fig.2, p4-10, p11-19  |Paleoarchean|Paleoarchean|Coppin Gap Greenstone Belt. Lithology described in some detail. REE and La/Yb contents detailed.|3470-3461 Ma.|Of the Warrawoona Group||Overlies Mount Ada Basalt. Is overlain by Towers Formation.|Includes intermediate to felsic volcanic rock, dominantly plagioclase porphyry; white dolomite; ferruginous and non-ferruginous greenish-grey silt-sized laminated chert; quartz-feldspar porphyry; and banded iron formation.|
5770|Duffer Formation|63245|5|Briefly described|p4 Fig. 1, p5 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3465ma. Geological Province: Pilbara Craton. Felsic volcanics.||||||07-NOV-08
5770|Duffer Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Coongan Subgroup (Warrawoona Group, Pilbara Supergroup). Age: c. 3465Ma. Geological Province: Pilbara Craton. Felsic volcanic rock; local basalt, chert and felsic schist; metamorphosed.||||||07-NOV-08
5770|Duffer Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Coongan Subgroup (Warrawoona Group, Pilbara Supergroup). Contains the Marble Bar Chert Member.  Age: c.3474-3463Ma. Geological Province: Pilbara Craton. Felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed.||||||07-NOV-08
5770|Duffer Formation|63441|5|Briefly described|p4 Tb. 1, p19|Archean|Archean|Of Coongan Subgroup (Warrawoona Group, Pilbara Supergroup). Age: 3474-3463Ma. Geological province: Pilbara Craton.||||||07-FEB-11
5770|Duffer Formation|63538|4|Described|p3 Fig. 2, p8 Tb. 1, p9, p13, p1|Archean|Archean|Of Coongan Subgroup (Warrawoona Group). Overlies Mount Ada Basalt conformably, overlain by Apex Basalt. Age: c. 3474-3463 Ma. Geological Province: Pilbara Craton. Basalt-dacite.||||||19-APR-13
5770|Duffer Formation|63649|5|Briefly described|p201 Fig. 2|Archean|Archean|Of the Warrawoona Group (Pilbara Supergroup). Age: 3.471 - 3.463Ga. Geological Province: Pilbara Craton.||||||07-FEB-11
5770|Duffer Formation|64328|5|Briefly described|p55|Archean|Archean|Age: c.3470-3465Ma.||||||07-FEB-11
5770|Duffer Formation|64405|5|Briefly described|p6, p13, p15|Archean|Archean|Age: 3471-3465Ma. Felsic volcanic rocks. See also p4 Fig. 3.||||||07-FEB-11
5770|Duffer Formation|64580|4|Described|map legend||Paleoarchean|Of Coongan Subgroup. Felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed.||||||09-DEC-08
5770|Duffer Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of the Coongan Subgroup (Warrawoona Group). Contains Marble Bar Chert and Chinaman Pool Chert Members. Felsic volcanic rock, local basalt, chert, and felsic schist; metamorphosed.||||||05-SEP-14
5770|Duffer Formation|64628|5|Briefly described|p169, p170, p171 Fig.1, p178.  |Archean|Archean|Pilbara Craton. Similar to the dacitic precursor to the Kittys Gap chert.|c.3.4 Ga.|Unit in Warrawoona Group.|||Dacites and andesites.|
5770|Duffer Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Talga Talga Subgroup (Warrawoona Group). Geological Province: Pilbara Craton. Undivided metamorphosed felsic volcanic and sedimentary rocks.||||||07-FEB-11
5770|Duffer Formation|64747|6|Mentioned|p94 fig 1, p115, p119|Paleoarchean|Paleoarchean|Part of an East Pilbara-wide episode of voluminous felsic volcanic-plutonic activity. No zircons from this event were found in the Dresser Formation, implying deposition of that unit before 3470 Ma.|3470-3460 Ma.|Unit in Warrawoona Group.|Includes Marble Bar Chert Member.|||
5770|Duffer Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Talga Talga Subgroup. Over Mount Ada Basalt; under Marble Bar Chert Member. Age: 3474-3463 Ma (geochron: NJ McNaughton etal 1993; others). Dacite, andesite, volcanogenic units, basalt. Geol. Prov: East Pilbara Granite-Greenstone Terrane, Pilbara Craton||||||
5770|Duffer Formation|65008|5|Briefly described|p9|||East Pilbara Granite-Greenstone Terrane.||Of the Talga Talga Subgroup|||Undivided metamorphosed felsic volcanic and sedimentary rocks.|
5770|Duffer Formation|65726|5|Briefly described|Map legend|Archean|Archean|East Pilbara Granite-Greenstone Terrane, Pilbara Craton.|c.3465 Ma (Buick 2002).|Of Talga Talga Subgroup. ||Intruded by Apex Basalt.|Mapped as two sub-units: metamorphosed felsic volcanic and sedimentary rock; quartzic schists, sheared metamorphosed dacitic lava and tuff.|
5770|Duffer Formation|65727|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Mapped as four sub-units.|c.3465 Ma (Thorpe et al. 1992).|Of Coongan Subgroup. |||Felsic volcanic rock, local basalt, chert and felsic schist; mafic schist after komatiitic basalt; quartzic schist, sheared dacitic lava and volcaniclastic rocks; interlayered psammitic and pelitic schist, metamorphosed shale, siltstone, sandstone.|
5770|Duffer Formation|65827|3|Fully described|p12 Tb.3, p13 Tb.4, p17, p19, p58-59|Paleoarchean|Paleoarchean|Of Coongan Subgroup; formerly of Talga Talga Subgroup. 3465 +/- 3 Ma (conventional zircon U-Pb; Thorpe et al. 1992). Intruded by Kennell, Chessman and Wilina Granodiorites, Homeward Bound Granite; unconformably underlies Apex Basalt; overlies Mount Ada Basalt. Faulted, concordant contact with Underwood Gneiss. Felsic volcanics; includes quartz-muscovite-andalusite-kyanite schist. Hosts gold-bearing quartz veins near Yandicoogina, and the Lennons Find Zn-Cu-Pb-barite VHMS deposit.||||||
5770|Duffer Formation|66108|5|Briefly described|Map legend|Paleoarchean|Paleoarchean|Unit in Coongan Subgroup. Felsic volcanic rock; local basalt, chert and felsic schist; metamorphosed. Includes Marble Bar Chert Member and an unnamed unit of metamorphosed massive feldspar-porphyritic dacite and andesite with subvolcanic intrusive rocks.||||||
5770|Duffer Formation|66217|3|Fully described|p1, p8, p15, p17, pp19-24, p60.|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Included in the Talga Talga Subgroup by Van Kranendonk et al. (2002). Type area is the creek flowing W to E into the Coongan River, 14 km north of Marble Bar. Up to 8000 m thick. Hosts historic massive sulfide (Cu-Pb-Zn) deposits at Doolena Gap. Has ages from 3477 (max depositional age) to 3463 (eruption of basal unit) Ma.|3463 +/- 2 Ma U/Pb SHRIMP (Nelson 2000b).|Upper unit in Coongan Subgroup.|Includes Marble Bar and Chinaman Pool Chert Members.|Conformably overlies, and interfingers with, Mount Ada Basalt. Is intruded by Apex Basalt feeder dykes. Is overlain disconformably by Panorama Formation, and unconformably by Strelley Pool Formation.|Predominantly dacitic volcaniclastic rocks; grades up to rhyolite; feldspar-porphyritic subvolcanic intrusions are common and voluminous; also pillow basalt and layered red and white sedimentary chert.|27-JAN-17
5770|Duffer Formation|66664|5|Briefly described|p7, p9.||||||Includes Marble Bar Chert Member and an unnamed unit of felsic schist.||Felsic volcaniclastic rocks; local felsic intrusive rocks; local sandstone and conglomerate.|
5770|Duffer Formation|66745|3|Fully described|p53 Fig.3, p54 Fig.4.|Paleoarchean|Paleoarchean|Explosive felsic volcanic complexes up to 8 km thick; debris flows common. Base metal mineralization.|3471-3463 Ma.|Unit in Coongan Subgroup.|Includes Marble Bar Chert Member.|Overlies Mount Ada Basalt. Is overlain by Panorama Formation in western Warralong, Panorama and Coongan greenstone belts; in other greenstone belts, is overlain by Apex Basalt.|Felsic volcanic rocks; minor basalt, siliciclastic rocks, jaspilite.|
5770|Duffer Formation|67130|5|Briefly described|p13, p53, p58, p75|Paleoarchean|Paleoarchean||3474 - 3463 Ma|Warrawoona Group|Includes Marble Bar Chert Member, Chinaman Pool Chert Member|Disconformably overlies Mount Ada Basalt,  Antarctic Creek Member, overlain by Marble Bar Chert Member|Dacite dominated deposit up to 8km thick. Basaltic Komatiitic pillow lavas|
5770|Duffer Formation|67197|5|Briefly described|p4|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coongan Subgroup.|Marble Bar Chert Member.|||
5770|Duffer Formation|67201|4|Described|p7 Fig.4, p12 Tb.1|||In northern Pilbara Craton, East Pilbara Terrane.|c. 3465 Ma|Coongan Subgroup||||
5770|Duffer Formation|67269|5|Briefly described|p5, p6 Fig.3, p13|Paleoarchean|Paleoarchean||3471-3463 Ma.|Coongan Subgroup.|Marble Bar Chert Member.|Overlies Mount Ada Basalt. Is overlain by Panorama Formation.|Felsic volcanic rocks and chert.|
5770|Duffer Formation|67270|5|Briefly described|p4, p6, p18|Paleoarchean|Paleoarchean|East Pilbara Terrane.|3471-3463 Ma.|Coongan Subgroup.|Marble Bar Chert Member.|||
5770|Duffer Formation|67668|6|Mentioned|Fig. 2; p. 154||Paleoarchean|East Pilbara Terrane, Pilbara Craton.|3472 - 3465 Ma|Warrawoona Group||Overlies the Mount Ada Basalt, underlies the Marble Bar Chert.||
5770|Duffer Formation|68035|4|Described|p288 Fig 4, p294|Paleoarchean|Paleoarchean|Warrawoona Group, Pilbara Supergroup, East Pilbara Terrane. Includes volcanic-hosted massive sulfides (Cu-Pb-Zn, with 20% barite).|3471-3463 Ma|Of Coongan Subgroup.|Includes Marble Bar Chert Member.|Overlies and in part laterally equivalent to Mount Ada Basalt. Disconformably overlain by Apex Basalt, Panorama Formation.|Felsic volcanic rocks, lesser siliciclastic rocks, minor basalt, jaspilite.|
5770|Duffer Formation|68280|4|Described|p2, p4, p11, p27, p30, p32, p35||||3471-3463 Ma|Coongan Subgroup|Includes Marble Bar Chert Member, Chinaman Pool Chert Member|Overlies Mount Ada Basalt, disconformably overlain by Apex Basalt|Felsic volcanic rocks, basalt, jaspilite and siliciclastic rocks, felsic agglomerate or volcaniclastic conglomerate. Porphyritic dacite.|
5770|Duffer Formation|68281|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Detailed lithology discussed in map legend; the 3 facies are mapped separately. Ages from Thorpe et al. (1992) and McNaughton et al. (1993).|3471-3463 Ma |Of the Coongan Subgroup.|Includes Marble Bar Chert Member.||Fine-grained felsic volcanic sandstone; layered or massive chert; sandstone and siltstone with volcanic clasts; massive to thickly bedded and partly silicified quartzose sandstone; all metamorphosed; felsic schist derived from felsic volcanic rocks.|
5770|Duffer Formation|68283|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton.|c.3474-3463 Ma|Of the Coongan Subgroup.|Includes Marble Bar Chert Member.||Felsic volcanic rock, local basalt, chert, and felsic schist; red, white and grey layered chert; massive feldspar porphyritic dacite, grades to andesite, includes subvolcanic intrusive rock; all metamorphosed.|
5770|Duffer Formation|68284|5|Briefly described|p4, 7|Paleoarchean|Paleoarchean|Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|3471-3463 Ma.|Coongan Subgroup (Warrawoona Group).|Marble Bar Chert Member.|Overlies Mount Ada Basalt. Is overlain by Apex Basalt.||
5770|Duffer Formation|69012|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane. Six other unnamed sub-units are mapped separately.|3471-3463 (McNaughton et al., 1993)|Of the Coongan Subgroup.|Includes the Marble Bar Chert Member.||Comprises felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed.|28-APR-14
5770|Duffer Formation|69015|5|Briefly described|Map Legend|Paleoarchean|Paleoarchean|East Pilbara Terrane, Pilbara Craton. Geochronology by Thorpe et al. (2002) and McNaughton et al. (1993). Also includes 4 unnamed sub-units mapped separately.|3471-3463 Ma|Of the Coongan Subgroup.|Includes the Marble Bar Chert Member.||Felsic volcanic rock, local basalt, chert, and felsic schist; sandstone and minor conglomerate; fine-grained felsic volcanic sandstone, local chert, wacke and conglomerate; felsic volcanic breccia, locally schistose; all metamorphosed.|02-MAY-14
5770|Duffer Formation|69041|4|Described|p12|Archaean|Archaean|Crops out along the northern margin of the Mount Edgar Igneous Complex. Defined and described by Lipple (1975).|ca 3470 Ma (Thorpe et al, 1992)|||Disconformably overlies the Mount Ada Basalt and Coppin Gap Suite.|Dacitic lava, tuff and pyroclastic fall depsoits with subordinate rhyolite, basalt, chert and porphryitic intrusions. Hornblende plagioclase schist and metamorphosed volcanic, mafic intrusives and sedimentary rocks also occur.|
5770|Duffer Formation|69167|4|Described|geologyp_lut.csv|Paleoarchean|Paleoarchean|Age derived from samples of felsic volcanic unit and porphyritic dacite (142975.1.pdf, 168920.1.pdf). Intruded by unnamed quartz diorite phase.|3474 +/- 7 Ma -3467 +/- 5 Ma(SHRIMP)|Coongan Subgroup|Includes Marble Bar Chert Member, Chinaman Pool Chert Member|Overlies Mount Ada Basalt|Felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed|
5770|Duffer Formation|69185|4|Described|GEOL_LUT_CSV files||Paleoarchean|Geological province: East Pilbara Granite-Greenstone Terrane, Pilbara Craton. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Coongan Subgroup.|||Felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed|
5770|Duffer Formation|69301|4|Described|p5 Fig.3, p8, p9 Tb.1, p10-11, p20 Tb.2|||Pilbara Craton. East Pilbara Terrane. Thickness: 8 km. Geochronology has confirmed a previous interpretation (Reynolds et al. 1975; Hickman & Lipple 1978) that Homeward Bound Granite is a sub-volcanic intrusion associated with Duffer Formation. Pilbara Supergroup successions include thick felsic volcanic formations, each contemporaneous with the four granitic supersuites. i.e. Duffer Formation and Callina Supersuite.|3471-3463 Ma Hickman&Van Kranendonk 2008; 3465 Ma|Coongan Subgroup|Marble Bar Chert Member|Disconformity at top. Is intruded by Homeward Bound Granite (Callina Supersuite).|Volcanic pile. Mainly felsic volcanic rocks; with siliciclastic rocks, basalt, jaspilite.|
5770|Duffer Formation|69566|5|Briefly described|p236-238|||East Pilbara Granite-Greenstone Terrane. Age range 3471-3463 Ma.|3468 +/- 2 Ma (Nelson, 2001).|Warrawoona Group.||Overlies Mount Ada Basalt. Is overlain by Apex Basalt.|Felsic. Includes a staurolite-garnet-bearing felsic schist.|
5770|Duffer Formation|69569|6|Mentioned|p285 Figs.1,2|||East Pilbara Terrane.||Warrawoona Group.||||
5770|Duffer Formation|69590|4|Described|GEOL_LUT_CSV files + geochron files|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton, West Australian Craton. Events: East Pilbara Terrane Rifting Event; Emu Pool Event; North Pilbara Orogeny; Prinsep Orogeny; Split Rock Supersuite; Warrawoona Event. Sample GSWA 142975 (crystal-lithic tuff) yielded an interpreted igneous crystallisation age of 3474+\-7 Ma (weighted mean 207Pb/206Pb). Sample GSWA 148503 (porphyritic tuffaceous rhyolite) yielded an interpreted igneous crystallisation age of 3433+\-2 Ma for the rhyolite (weighted mean 207Pb/206Pb). Sample GSWA 148509 (porphyritic tuffaceous andesite) yielded an interpreted igneous crystallisation age of 3468+\-2 Ma for the andesite (weighted mean 207Pb/206Pb). Sample GSWA 168918 (volcaniclastic sandstone) yielded an interpreted igneous crystallisation age of 3470+\-5 Ma for the volcaniclastic sandstone (weighted mean 207Pb/206Pb). Sample GSWA 168921 (felsic agglomerate) yielded an interpreted igneous crystallisation age of 3468+\-5 Ma for the agglomerate (weighted mean 207Pb/206Pb). See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.|3477-3463 Ma (inferred)|Unit of Coongan Subgroup.|Includes Chinaman Pool Chert Member, Marble Bar Chert Member.|Underlain by Mount Ada Basalt.|Dacite, dacitic volcanic breccia, andesite, andesite tuff, volcaniclastic sandstone, basalt, chert, dolerite, amphibolite, psammitic and pelitic schist, rhyolite, sandstone, siltstone, shale, BIFs.|
5770|Duffer Formation|69989|6|Mentioned|p26|Paleoarchean|Paleoarchean|North Pole Dome area, Pilbara Craton.|3.47 Ga.|Warrawoona Group.||||
5770|Duffer Formation|70022|6|Mentioned|p113, 115|||East Pilbara Terrane.|3.46 Ga.||||Includes rhyolite with zircon xenocrysts.|
5770|Duffer Formation|70507|5|Briefly described|p431|Archean|Archean|Geological province: Pilbara Craton.||Unit of Pilbara Supergroup.||||
5770|Duffer Formation|70729|5|Briefly described|p163,165|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.|c. 3.47 Ga||Includes Marble Bar Chert.|||
5770|Duffer Formation|70733|5|Briefly described|p103-104, 106-107, 120|||Marble Bar greenstone belt, East Pilbara Craton. Over 5km thick.|Between 3474 and 3459 +/- 2 Ma.|Warrawoona Group.|Marble Bar Chert Member.|Is overlain by Apex Basalt.|Felsic volcanics.|
5770|Duffer Formation|70775|5|Briefly described|p12, p101|Paleoarchean|Paleoarchean|East Pilbara.|c. 3465 Ma|Warrawoona Group||Overlies the Mount Ada Basalt. Overlain by the Apex Basalt.||
5770|Duffer Formation|70834|6|Mentioned|p298|Paleoarchean|Paleoarchean|Marble Bar greenstone belt, Pilbara Craton.|3468-3465 Ma.|||Overlies Mount Ada Basalt. Is overlain by Marble Bar Chert.|Dominantly felsic volcanics; some basalt, less siliciclastics.|
5770|Duffer Formation|70884|4|Described|p123-126,128-131,133-137|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.  Characterised by abrupt absence of basaltic volcanism compared to underlying Mount Ada Basalt. Thickness of up to ~580m in the central part of the study area, pinching out to the west under an angular unconformity. Felsic volcanism restricted to the east; more authigenic tuffs and volcaniclastic sediments to the west with finer-grained laminated siltstones and mustones and interbedded turbidites associated with basin deepening and sediment influx from the east. Late-stage Duffer Formation deposition associated with crustal uplift due to emplacement of Muccan Granitic Complex, and erosion of Warrawoona Group sediments. Silicification observed within felsic rocks in shear zones in the Low-Strain belt. Contains  3.31 Ga metamorphic zircon ages (U-Pb SHRIMP; Nelson, 1999; Fran¿ois et al., 2014), and possibly  3.33 Ga hydrothermal zircon (U-Pb SHRIMP; McNaughton et al., 1993), associated with D3 deformation post-Strelley Pool Formation.|3.47-3.46 Ga|Unit of Coongan Subgroup.||Overlain by Marble Bar Chert Member. Underlain by Mount Ada Basalt.|Volcaniclastic sediments, felsic volcanics, mafic sills and intrusions, cherts and stromatlites, altered spinifex-textured pillow basalt flows.|16-AUG-19
5770|Duffer Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoarchean|Paleoarchean|Warrawoona  Large Igneous Province.|Max age 3474+/-7 Ma, min 3459+/-2 Ma.|Coongan Subgroup|Includes Marble Bar Chert Member.||Felsic volcanic rock; local basalt, chert, and felsic schist; metamorphosed.|
5770|Duffer Formation|72064|5|Briefly described|p66|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton.||Unit of Warrawoona Group.|Includes Marble Bar Chert Member.|Overlain unconformably by Panorana Formation or Apex Basalt. Underlain by Mount Ada Basalt.||
5770|Duffer Formation|72251|5|Briefly described|p53-54|Paleoarchean|Paleoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Includes felsic extrusive units contemporaneous with the Callina Supersuite.||Unit of Coongan Subgroup.||Upper unit of Coongan Subgroup. Overlain by Apex Basalt. Underlain by Mount Ada Basalt.||
5770|Duffer Formation|72668|5|Briefly described|p3-6, p8-9, p19, p24, p27|||East Pilbara Terrane. Geochemistry is discussed.|c. 3471-3463 Ma|Coongan Subgroup||Overlies the Mount Ada Basalt.|basalt to dacite dominated deposits with rare rhyolites.|13-JAN-22
5770|Duffer Formation|73598|6|Mentioned|p1212|Paleoarchean|Paleoarchean|East Pilbara Terrane.||Coongan Subgroup.||Overlies Mount Ada Basalt. Is overlain by Apex Basalt.||
5780|Dugel Gneiss|22694|5|Briefly described|p6|Archean|Archean|||||||07-NOV-08
5780|Dugel Gneiss|23569|4|Described|p5 Tb. 1|Archean|Archean|Of the Narryer Terrane.   Monzogranitic and syenogranitic gneiss.  See also p6 Tb. 1.||||||07-NOV-08
5780|Dugel Gneiss|23574|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Milga Gneiss. Underlying unit Eurada Gneiss.||||||07-NOV-08
5780|Dugel Gneiss|23576|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Milga Gneiss. Underlying unit Eurada Gneiss.||||||07-NOV-08
5780|Dugel Gneiss|23577|5|Briefly described|Map Legend|Archean|Archean|Overlying unit Milga Gneiss. Underlying unit Eurada Gneiss.||||||07-NOV-08
5780|Dugel Gneiss|23781|4|Described|p14|Archean|Archean|Age: 3385-3300Ma (SHRIMP U-Pb).||||||07-NOV-08
5780|Dugel Gneiss|24114|5|Briefly described|p5 Fig.4|Archean|Archean|Geological Province: Yilgarn Craton. Age: 3400-3300 Ma||||||07-NOV-08
5780|Dugel Gneiss|24160|6|Mentioned|p64|||Narryer Terrane. This unit's protoliths intruded the Meeberrie Gneiss. Contains inclusions of Manfred Complex rocks.|3.4 Ga.|Unit in Narryer Gneiss Complex.|||Metamorphosed leucocratic syenogranite and monzogranite.|
5780|Dugel Gneiss|40587|6|Mentioned|p350|||||||||
5780|Dugel Gneiss|41008|5|Briefly described|p358|||||||||
5780|Dugel Gneiss|41261|3|Fully described|p6|||||||||
5780|Dugel Gneiss|41991|5|Briefly described|p130|||||||||
5780|Dugel Gneiss|42159|5|Briefly described|p310|||See also Fig.1||||||
5780|Dugel Gneiss|42800|5|Briefly described|p68|||of Narryer Gneiss Complex||||||
5780|Dugel Gneiss|43835|5|Briefly described|Map Legend||Archean|Age: 3400-3300 Ma||||||07-NOV-08
5780|Dugel Gneiss|44149|4|Described|p15, p17-19, p22-24, p30|Paleoarchean|Paleoarchean|Myers and Williams (1985); Williams and Myers (1987). Derived from leucocratic syenogranite and monzogranite which intruded Meeberrie Gneiss. Other ages given. Encloses plagioclase megacrysts from Manfred Complex.|3381 +/- 22 Ma (Zircon U-Pb; Kinny et al., 1988).|Narryer Gneiss Complex||Intruded Meeberrie Gneiss. Not obviously distinct from Manfred Complex in some places.|Quartzo-feldspathic gneiss; syenogranitic or monzogranitic in composition; generally leucocratic. Amphibolite facies metamorphosed. Where undeformed contains blebby textures and irregular patches or veins of partial melting.|
5780|Dugel Gneiss|49896|6|Mentioned|p18|Archean|Archean|Age: 3375+/-26Ma.||||||07-NOV-08
5780|Dugel Gneiss|50216|5|Briefly described|p203|Archean|Archean|Age: 3385-3300 Ma. Geological Province: Narryer Terrane in the northwestern part of Yilgarn Craton.||||||07-NOV-08
5780|Dugel Gneiss|66299|4|Described|p28.|Archean|Archean|Narryer Terrane, Yilgarn Craton. Contains abundant dismembered sheets of metagabbro-metadolerite and metaperidotite.|3400-3300 Ma.||||Quartz-K-feldspar-plagioclase(-biotite) syenogranitic gneiss and monzogranite, with pegmatite layering or veins.|
5780|Dugel Gneiss|67129|4|Described|p3-4|Archean|Archean|Narryer Terrane. Widespread unit. Hosts the Manfred Complex. Also 3284 +/-9 Ma zircon rims (Nutman et al., 1991).|3375 +/- 26 Ma (SHRIMP upper intercept)|||Crosscuts Meeberrie Gneiss.|Dominantly syenogranite, ranging to monzogranite in composition.|06-SEP-17
5780|Dugel Gneiss|67855|6|Mentioned|p198, p200 fig 3-3, p201||||3400 Ma|Narryer Gneiss Complex||||
5780|Dugel Gneiss|68123|6|Mentioned|p30, 32, 35-38|Archean|Archean|Narryer Terrane, Yilgarn Craton. Detrital zircons age peaks.|c.3380-3350 Ma.|||Intrudes Meeberrie Gneiss.||
5780|Dugel Gneiss|69583|5|Briefly described|p54|||Underwent deformation, and amphibolite to granulite facies metamorphism, at c.3300 Ma.||||Intrudes the Meeberrie Gneiss and Manfred Complex.|Syenogranitic; includes leucogabbro and meta-anorthosite inclusions from the Manfred Complex.|
5780|Dugel Gneiss|70020|5|Briefly described|p116|Paleoarchean|Paleoarchean|Geological province: Yilgarn Craton. Felsic magmatic intrusion in the Meeberie Gneiss.|c. 3.3 Ga|||||
5780|Dugel Gneiss|71168|5|Briefly described|p6|Paleoarchean|Paleoarchean|Narryer and South West Terranes, Yilgarn Craton.|c. 3300 Ma|||Intrudes the Manfred Complex and the Meeberrie Gneiss.||
5780|Dugel Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||amphibolite, gabbro, felsic gneiss|
5780|Dugel Gneiss|71269|6|Mentioned|1m_geologyp12_lut.csv|||Of Narryer Gneiss Complex.|||||Monzogranitic and syenogranitic gneiss, in places with abundant amphibolite and metagabbro inclusions|
5780|Dugel Gneiss|73526|5|Briefly described|p2 Fig.1, p3|Paleoarchean|Paleoarchean|Minor part of the central Narryer Terrane.|3400-3300 Ma||||Metamorphosed monzogranite and syenogranite.|
5795|Dumbardo Siltstone|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Of the Lyons Group. Underlying unit: Coyango Greywacke. Overlying unit: Koomberan Greywacke.||||||
5795|Dumbardo Siltstone|32648|6|Mentioned|p32|||Lyons Gp.||||||
5795|Dumbardo Siltstone|36890|6|Mentioned|p279|||||||||
5795|Dumbardo Siltstone|37295|6|Mentioned|Table 2|||||||||
5795|Dumbardo Siltstone|41271|6|Mentioned|p65|||||||||
5795|Dumbardo Siltstone|44344|14|Not recorded|p.6-8,24,opp.4,map|||Sakmarian in age. (G50-1).||||||
5795|Dumbardo Siltstone|44345|14|Not recorded|map legend||Sakmarian|||||||
5795|Dumbardo Siltstone|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group.||||||01-JUN-06
5795|Dumbardo Siltstone|45016|2|Defined|p.32-36||Sakmarian|Tb, p.7,9,12,13,15,16,22,27,28,Fig.48,37,39,48,F.50. (F50-13 -type area).||||||
5795|Dumbardo Siltstone|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
5859|Duplex Hill Group|41249|6|Mentioned|Fig.11|||||||||
5872|Durba Sandstone|22816|5|Briefly described|p8 Table 1|||Savory Group.||||||28-JUL-08
5872|Durba Sandstone|22907|6|Mentioned|40|||||||||
5872|Durba Sandstone|23730|5|Briefly described|p6, 13|Neoproterozoic|Neoproterozoic|Of Disappointment Group. Geological Province: Officer Basin.||||||
5872|Durba Sandstone|24161|6|Mentioned|p29|||||||||
5872|Durba Sandstone|24390|5|Briefly described|p11 Fig. 6|Cambrian|Cambrian|Geological Province: Officer Basin.||||||
5872|Durba Sandstone|33849|4|Described|p126|||||||||
5872|Durba Sandstone|35596|4|Described|p11|||||||||
5872|Durba Sandstone|37020|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5872|Durba Sandstone|37022|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
5872|Durba Sandstone|37214|3|Fully described|p9|||||||||22-DEC-09
5872|Durba Sandstone|37460|5|Briefly described|p173|||||||||
5872|Durba Sandstone|37707|5|Briefly described|p20|||||||||
5872|Durba Sandstone|38898|6|Mentioned|p83|||||||||
5872|Durba Sandstone|40089|2|Defined|p59|Mesoproterozoic|Mesoproterozoic|||||||
5872|Durba Sandstone|42708|5|Briefly described|Plate 1|Proterozoic||||||||
5872|Durba Sandstone|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||11-APR-08
5872|Durba Sandstone|43492|4|Described|9|||||||||
5872|Durba Sandstone|43756|5|Briefly described|Fig.1,p535,p540-41|||||||||
5872|Durba Sandstone|44111|6|Mentioned|p.58, Fig. 2|||in Savory Basin. Appears in text as Durba (no lithology).||||||
5872|Durba Sandstone|50085|5|Briefly described|p11 Fig. 6|Ordovician|Ordovician|Age: <500Ma.  Geological Province: Officer Basin.||||||
5872|Durba Sandstone|50188|5|Briefly described|p10 Fig. 3|Cambrian|Cambrian|Age: ?520Ma. Geological Province: Earaheedy Basin.||||||28-JUL-08
5872|Durba Sandstone|61023|5|Briefly described|p15 Fig. 8|Ordovician|Ordovician|Geological Province: Gunbarrel Basin.||||||10-APR-08
5872|Durba Sandstone|61732|5|Briefly described|p85, p89||Ediacaran|Overlies the Diasappointment Group units unconformably. Geological Province: northeastern Officer Basin.||||||07-FEB-11
5872|Durba Sandstone|62453|3|Fully described|p5 Fig. 3, 22, 62|Ediacaran|Ediacaran|Geological Province: Officer Basin. Overlies McFadden and Boondawari Formation. Underlies Paterson Formation. Thickness less than 100m. Conglomerate, sandstone.||||||17-JUL-08
5872|Durba Sandstone|62987|5|Briefly described|p30|||Overlies McFadden and Lungkarta Formations. Geological Province: Officer Basin. Fluvial deposits.||||||
5872|Durba Sandstone|63022|5|Briefly described|p1015|||Aeolian-dominated sandy succession with a fluvial cap. Geological Province: Officer Basin.||||||16-JUL-13
5872|Durba Sandstone|64103|6|Mentioned|p400, p400 Fig. 3, p401|Cambrian|Ediacaran|Geological Province: Officer Basin.||||||07-FEB-11
5872|Durba Sandstone|64283|5|Briefly described|p50 Fig. 1|||Geological Province: Oldham Inlier.||||||07-FEB-11
5872|Durba Sandstone|64580|4|Described|map legend||Ediacaran|Sandstone, pebbly in places; minor conglomerate.||||||09-DEC-08
5872|Durba Sandstone|64772|5|Briefly described|p15-16, Plate 1, p14 Fig. 7, p20-21|Neoproterozoic|Neoproterozoic|Unconformable on McFadden Fm. Oldham Inlier area. Restricted to a few small outliers scattered along the northeastern margin of TRAINOR. Officer Basin, Centralian Superbasin. Unknown age, although tectonic models and stratigraphic relationships imply that it is related to the Paterson Orogeny at about 550 Ma (Grey et al., 2005)|||||Upward-fining seq.of basal sandstone, polymictic pebble to cobble conglomerate up to 1m thick; overlain by red-brown coarse- to medium-gr.sandstone, + few scattered pebbles|25-NOV-13
5872|Durba Sandstone|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Savory Basin. Overlies Savory Group?||||||
5872|Durba Sandstone|65363|5|Briefly described|p5 Fig.4, pp12-14, p19.|Ordovician|Ordovician|Officer Basin. Shown repeatedly in this report as Lennis / Durba Sandstone, presumably for reasons of space. Northwestern Officer Basin. May correlate with Lennis Sandstone in the south of the basin.||||Overlies Table Hill Volcanics. Is unconformably overlain by Paterson Formation.||
5872|Durba Sandstone|65364|5|Briefly described|p81|||Officer Basin.||||Overlain by Paterson Sandstone, underlain by Lungkarta Formation.|Pale brown quartz-rich cross-bedded sandstone.|16-MAR-12
5872|Durba Sandstone|65366|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|||||||19-MAR-12
5872|Durba Sandstone|65371|5|Briefly described|p54 Fig. 1|||Conformable on Lungkarta Formation. Unconformably overlain by Paterson Formation. Pale brown sandstones of the Officer Basin, probably fluvial depositional environment||||||
5872|Durba Sandstone|65416|4|Described|p137, p138 Fig.3, p144, p146.|Middle Cambrian|Middle Cambrian|Officer Basin. Part of Sequence LP4B of Supersequence LP4, but this needs further investigation. Fluvial, arid fan environment. Now includes sandstone and claystone betweeen 100 and 465 m in Hussar 1, previously interpreted as Lennis Sandstone and Wanna Formation.||||Overlies McFadden and Boondawari Formations unconformably.|Clean quartz sandstone, minor basal conglomerate lenses and claystone.|
5872|Durba Sandstone|67454|5|Briefly described|p563. |Paleozoic|Neoproterozoic|Officer Basin.||||Overlies Lungkarta Formation. Is overlain by Paterson Formation.||
5872|Durba Sandstone|69003|5|Briefly described|p60, p62|Cambrian|Cambrian|NW Officer Basin. Caps the Durba Hills.||||Overlies McFadden Formation.||
5872|Durba Sandstone|70839|6|Mentioned|p342-343|Early Cambrian|Ediacaran|Of West Officer Basin. Age is broadly constrained between Ediacaran to early Cambrian based on stratigraphic position (Grey et al., 2005).||||||
5872|Durba Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
5872|Durba Sandstone|71618|6|Mentioned|p131|Cambrian|Cambrian|Of Officer Basin. Fluvial depositional environment, with similar zircon age spectra to the Decoration Sandstone.||||||
5872|Durba Sandstone|71800|5|Briefly described|p26-p27|Middle Cambrian|Middle Cambrian|Officer Basin.|||||Pebbly quartz arenite.|
5872|Durba Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Ediacaran|Officer Basin (Phase 1).||Disappointment Group|||Sandstone, lesser pebble congomerate; characteristically purplish red-brown colour.|
5885|Dyasons Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1860Ma. Geological province: Kimberley Province (West).||||||07-FEB-11
5885|Dyasons Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
5885|Dyasons Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
5885|Dyasons Granite|30533|5|Briefly described|Table 1|||See also p14.||||||14-NOV-06
5885|Dyasons Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
5885|Dyasons Granite|32728|6|Mentioned|Table 4|||||||||
5885|Dyasons Granite|36885|4|Described|p174|||||||||
5885|Dyasons Granite|37633|6|Mentioned|p97|||||||||
5885|Dyasons Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
5885|Dyasons Granite|42811|5|Briefly described|p11|||||||||
5885|Dyasons Granite|43281|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Approx 1865 - 1850 Ma.||||||07-NOV-08
5885|Dyasons Granite|44155|4|Described|p242 Tb.3-5|||||Hooper Complex||Intrudes McSherrys Granodiorite and Lennard Granite. Is intruded by Mount Amy Granite.|Grey, medium to fine, even-grained, biotite granite with abundant mesocratic schlieren.|
5885|Dyasons Granite|50437|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite.||||||07-NOV-08
5885|Dyasons Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Paperbark Supersuite.|||Recrystallised leucocratic medium to fine grained biotite monzogranite with minor secondary muscovite|
5885|Dyasons Granite|72437|5|Briefly described|p65, p73-75|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Micro-monzogranite.|
5901|East Kimberley kimberlite|40811|6|Mentioned|p317|||||||||
5901|East Kimberley kimberlite|41158|6|Mentioned|p250|||||||||
5905|East Yilgarn Gneiss|38788|6|Mentioned|Fig.2|||||||||
5914|Eastern Gneiss|30011|5|Briefly described|p165|||||||||
5915|Eastern Lennard Shelf Lamproite|41158|6|Mentioned|Table 42|||||||||
5943|Echuca Shoals Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 16|Early Cretaceous|Early Cretaceous|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Also on p222, p228 Fig. 18.||||||01-MAR-10
5943|Echuca Shoals Formation|7142|6|Mentioned|p350 Fig.4.|Early Cretaceous|Early Cretaceous|Browse Basin.||||Overlies Upper Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|13267|6|Mentioned|pp274-279.|Early Cretaceous|Early Cretaceous|Barremian to Aptian.||||Overlies Flamingo Group. Is overlain by Darwin Formation.||
5943|Echuca Shoals Formation|13353|5|Briefly described|p398, p417.|Early Cretaceous|Early Cretaceous|Includes hydrocarbon source rocks. Characteristics of the W3 Petroleum System of this unit: richness, expulsion, migration conduits, reservoir/traps, seal facies, risks/assumptions etc, are detailed on p417.||||Overlies Upper Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|13354|6|Mentioned|p375 Fig.6.|Early Cretaceous|Early Cretaceous|Unit of Bathurst Island Group. Overlies Upper Vulcan Formation of the Swan Group, and underlies Jamieson Formation.||115||||28-OCT-14
5943|Echuca Shoals Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Early Cretaceous|Bathurst Island Group.||||||01-MAR-10
5943|Echuca Shoals Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Early Cretaceous|||||||
5943|Echuca Shoals Formation|23376|4|Described|p229 Fig.2; p244|Barremian|Valanginian|Of Bonaparte Basin.||||||15-AUG-06
5943|Echuca Shoals Formation|23378|4|Described|p180 Fig.2, p202||Early Cretaceous|Of Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||01-MAR-10
5943|Echuca Shoals Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
5943|Echuca Shoals Formation|24207|4|Described|p213|Barremian|Hauterivian|See also Echuca Shoals. Predominantly an extensive claystone. Geological Province: Vulcan Sub-basin.||||||01-MAR-10
5943|Echuca Shoals Formation|24234|5|Briefly described|p287 Fig.3|Early Cretaceous|Early Cretaceous|See also Echuca Shoals. Geological Province: Bonaparte Basin.||||||
5943|Echuca Shoals Formation|24379|5|Briefly described|p17|||Overlain by Wangarlu Formation. Geological Province: North west shelf.||||||14-APR-08
5943|Echuca Shoals Formation|24427|5|Briefly described|p49|Cretaceous|Cretaceous|||||||
5943|Echuca Shoals Formation|42053|4|Described|p42|||||||||01-MAR-10
5943|Echuca Shoals Formation|42056|4|Described|p100|||||||||
5943|Echuca Shoals Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
5943|Echuca Shoals Formation|42861|6|Mentioned|p4|||||||||
5943|Echuca Shoals Formation|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
5943|Echuca Shoals Formation|60378|5|Briefly described|p95, Fig 2|Early Cretaceous|Early Cretaceous|Marine sediments. Petroleum seal.||||||
5943|Echuca Shoals Formation|60385|6|Mentioned|p269 to 271|Albian|Valanginian|Browse Basin.|||||Organic-rich, oil-prone marine shale.|
5943|Echuca Shoals Formation|60386|6|Mentioned|p302|Valanginian|Berriasian|Browse Basin, Bonaparte Basin. Distal shelf/basin.||||||
5943|Echuca Shoals Formation|60634|6|Mentioned|p1168 Fig.3. |Early Cretaceous|Early Cretaceous|||Unit in Bathurst Island Group.||Overlies Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Early Cretaceous|Northern Bonaparte Basin.||||||
5943|Echuca Shoals Formation|61550|6|Mentioned|p495 Fig.2. |Aptian|Berriasian|||Unit in Bathurst Island Group.||||
5943|Echuca Shoals Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Neocomian|Age: ~133-~114Ma. Geological Province:  Ashmore Platform.||||||01-MAR-10
5943|Echuca Shoals Formation|63358|5|Briefly described|p4 Fig. 1.3|Aptian|Valanginian|Mentions occur throughout the text. See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
5943|Echuca Shoals Formation|64689|5|Briefly described|p3, p8 Fig.7, p15-19, p20 Fig.20|Lower Cretaceous|Lower Cretaceous|Contains a previously interpreted oil system.||||||
5943|Echuca Shoals Formation|64696|6|Mentioned|p134, p138, p140 |||An important source interval in the Browse Basin. Source of a gas column in the Upper Vulcan Formation, in Kalyptea-1.||||||
5943|Echuca Shoals Formation|64697|5|Briefly described|p84 Fig.2|Early Cretaceous|Early Cretaceous|||||||
5943|Echuca Shoals Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Aptian|Valanginian|Bathurst Island Group. Underlies the Jamieson Formation, overlies the Upper Vulcan Formation. Mount Ashmore Dome. Deep water claystone.||||||
5943|Echuca Shoals Formation|68223|6|Mentioned|p178 Fig.3|Aptian|Valanginian|||||||
5943|Echuca Shoals Formation|69297|6|Mentioned|p303, p305, p309|Aptian|Berriasian|Barcoo and Seringapatam sub-basins of the Browse Basin. Transgressive and highstand depositional packages. May contain oil shows.  ||Bathurst Island Group||Overlies the Brewster Member of the upper Vulcan Formation.||
5943|Echuca Shoals Formation|69452|4|Described|p36:8, 15, 22|Cretaceous|Cretaceous|Pattillo and Nicholls, (1990). Deposited widely across the Bonaparte Basin. Offshore. Originally the basal Valanginian-Aptian interval of the Darwin Formation. >250m thick. Shallow marine deposits.||Bathurst Island Group.||Unconformably overlies Flamingo Group. Is overlain conformably by Darwin Formation.|Glauconitic claystone and siltstone.|12-JUL-16
5943|Echuca Shoals Formation|69456|5|Briefly described|p40:5|Early Cretaceous|Early Cretaceous|Bonaparte Basin. Valanginian-Barremian age.||Basal Bathurst Island Group.||||12-JUL-16
5943|Echuca Shoals Formation|69653|5|Briefly described|p6, 8, 10, 26-27, 38, 41-43, 50-51, 53|Cretaceous|Cretaceous|Petrel Sub-basin. Shoreface deposits. Schematic (gamma ray) well sections. Composite well diagram. See also p61, 63.||Bathurst Island Group.||Overlies Sandpiper Sandstone. Is overlain by Darwin Formation.|Medium-grained glauconitic sandstone with shale; mudstone interbedded with glauconitic siltstone/sandstone; mudstone with glauconitic sandstone. Facies described in detail.|
5943|Echuca Shoals Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Browse, Bonaparte Basins.||||Overlies Upper Vulcan Formation. Is overlain by Lower Jamieson Formation.||
5943|Echuca Shoals Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Aptian|Valanginian|See also Regional geology: Figs.6-7, p6, p10, p12, p14. Sahul: Fig.2, p1-3. Vulcan: Fig.2, p3. Potential source of wet gas and some light oil, such as that reservoired in the Darwin Formation. Forms a regional seal for hydrocarbons in the Vulcan Sub-basin, Sahul Syncline and N Bonaparte Basin. Source rock in Sahul Syncline.||Bathurst Island Group.||Overlies Sandpiper Sandstone. Is overlain by Darwin Formation.|Includes claystones.|12-JUL-16
5943|Echuca Shoals Formation|70064|5|Briefly described|Regional Fig.6; p4-7. Central:Fig.2;p1-2|Aptian|Valanginian|See also Northern: Fig.2; p1-2. Yampi: Fig.2; p1-2. Browse Basin. Contains organic-rich (mainly marine algae and bacteria) rocks with fair to moderate oil potential, and shallow marine sandstones and fans are potential reservoirs. It is also a regional seal (thick claystones). Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoirs in horsts and tilted fault-blocks.||Bathurst Island Group.||Overlies Upper Vulcan Formation. Is overlain by Lower Jamieson Formation.||12-JUL-16
5956|Edell Number I Trachyte|40811|4|Described|p321|||||||||
5995|Eerada Formation|29688|2|Defined|p43|Archean|Archean|||||||07-NOV-08
5995|Eerada Formation|29690|5|Briefly described|p7|||||||||
5995|Eerada Formation|30949|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
6057|Elgee Siltstone|22440|6|Mentioned|p5|||||||||
6057|Elgee Siltstone|22754|5|Briefly described|p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group||||||07-NOV-08
6057|Elgee Siltstone|23125|5|Briefly described|Table.1||Proterozoic|Age: Early Proterozoic. of Kimberley Group.||||||
6057|Elgee Siltstone|23383|5|Briefly described|p19, p18 Tb 2|||Of Kimberley Group. Contains Teronis Member. Mudstone. Siltstone, sandstone, dolomite, dolomitic siltstone.  Conformably overlain by Pentecost Sandstone; conformably overlies Warton Sandstone. Max. thickness: 250 m.  Geological Province: Kimberley Basin.||||||25-JAN-05
6057|Elgee Siltstone|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Kimberley Group.  Red-brown and grey siltstone and shale. Geological Province: Kimberley Basin.||||||07-NOV-08
6057|Elgee Siltstone|23621|6|Mentioned|p31|||||||||
6057|Elgee Siltstone|23722|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Parent: Kimberley Group.   Max. thickness: 180m.   Geological Province: Kimberley Basin.||||||09-DEC-08
6057|Elgee Siltstone|24173|5|Briefly described|p22, 23|Paleoproterozoic|Paleoproterozoic|May form part of the undivided Kimberley Group||||||07-NOV-08
6057|Elgee Siltstone|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group. Siltstone, shale, stromatolitic dolomite, sandy dolomite, oolitic dolomite and sandstone.  Geological Province: Kimberley Basin.||||||07-NOV-08
6057|Elgee Siltstone|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group.  Age: <1805Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
6057|Elgee Siltstone|29693|6|Mentioned|p100|||||||||
6057|Elgee Siltstone|29946|6|Mentioned|p253|||||||||
6057|Elgee Siltstone|30097|6|Mentioned|Table 23|||||||||
6057|Elgee Siltstone|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|30533|4|Described|p18|||On Table 3||||||
6057|Elgee Siltstone|30893|5|Briefly described|p193|||See also Fig. 1||||||
6057|Elgee Siltstone|30894|5|Briefly described|p250|||Carpentarian||||||
6057|Elgee Siltstone|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|30897|6|Mentioned|p13|||Stratigraphy||||||
6057|Elgee Siltstone|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6057|Elgee Siltstone|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
6057|Elgee Siltstone|31662|5|Briefly described|p255|||||||||
6057|Elgee Siltstone|32660|5|Briefly described|Table 3|||||||||
6057|Elgee Siltstone|32662|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|32663|4|Described|Table 1|||Carpentarian||||||
6057|Elgee Siltstone|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|32722|6|Mentioned|Fig.2|||Stromatolite||||||
6057|Elgee Siltstone|32728|5|Briefly described|p38|||||||||
6057|Elgee Siltstone|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|34137|4|Described|Table 1||Carpentarian|Carpentarian, part of Kimberley Group.||||||
6057|Elgee Siltstone|34190|4|Described|Table 1|||Proterozoic||||||
6057|Elgee Siltstone|34462|4|Described|Table 1|||Carpentarian||||||
6057|Elgee Siltstone|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6057|Elgee Siltstone|36551|4|Described|p28|||||||||
6057|Elgee Siltstone|36885|4|Described|p185|||||||||
6057|Elgee Siltstone|37228|6|Mentioned|Fig.2|||||||||
6057|Elgee Siltstone|38988|6|Mentioned|Fig.4|||||||||
6057|Elgee Siltstone|39116|6|Mentioned|p134|||||||||
6057|Elgee Siltstone|39210|6|Mentioned|Table 3|||||||||
6057|Elgee Siltstone|41158|6|Mentioned|p21|||||||||
6057|Elgee Siltstone|41703|6|Mentioned|Fig.2|||||||||
6057|Elgee Siltstone|41987|5|Briefly described|Fig.4 P74|||||||||
6057|Elgee Siltstone|42149|6|Mentioned|Table 1 P709|||||||||
6057|Elgee Siltstone|42710|5|Briefly described|map legend|Proterozoic||||||||
6057|Elgee Siltstone|42811|5|Briefly described|p23|||of Kimberley Group||||||
6057|Elgee Siltstone|42814|4|Described|p14|||Of Kimberley Group.||||||09-DEC-08
6057|Elgee Siltstone|42815|5|Briefly described|map|Proterozoic||||||||
6057|Elgee Siltstone|42821|6|Mentioned|p135|||||||||
6057|Elgee Siltstone|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Group.||||||
6057|Elgee Siltstone|43652|6|Mentioned|Fig.5,p383|||||||||
6057|Elgee Siltstone|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
6057|Elgee Siltstone|44140|4|Described|p295, p298, p300|Paleoproterozoic|Paleoproterozoic|40-480 m thick. Deformed c.600 Ma.||Kimberley Group|Includes Teronis Member.|Intruded by Wotjulum Porphyry|Distinctive, massive red siltstone, sandstone, green shale.|07-MAR-18
6057|Elgee Siltstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
6057|Elgee Siltstone|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Kimberley Group. Red-brown and grey siltstone and shale; minor quartz sandstone.  Geological Province: Kimberley Basin.||||||21-JUL-15
6057|Elgee Siltstone|44286|5|Briefly described|Map legend|||||||||
6057|Elgee Siltstone|44363|5|Briefly described|p.6,10,12,13,21,27|||(Carpentarian) Kimberley Group.||||||
6057|Elgee Siltstone|44364|14|Not recorded|map legend|||||||||
6057|Elgee Siltstone|44366|14|Not recorded|p.15||Carpentarian|Part of Kimberley Group.||||||
6057|Elgee Siltstone|44367|14|Not recorded|map legend|||(Reprinted 1971). Part of Kimberley Group.||||||
6057|Elgee Siltstone|44397|14|Not recorded|p.9, Table 2||Carpentarian|Kimberley Group.||||||
6057|Elgee Siltstone|44398|14|Not recorded|map legend||Carpentarian|||||||
6057|Elgee Siltstone|44694|5|Briefly described|Map Legend||Proterozoic|||||||
6057|Elgee Siltstone|45047|5|Briefly described|p28|||||||||
6057|Elgee Siltstone|45077|6|Mentioned|p7|||||||||
6057|Elgee Siltstone|48931|3|Fully described|p55|||||||||
6057|Elgee Siltstone|60714|5|Briefly described|p112, p113.  |||216m thick. Deposited in low palaeolatitudes (c.7.6 deg).||Unit in Kimberley Group.||Overlies Warton Sandstone. Is overlain by Pentecost Sandstone.|Massive red siltstone, sandstone and green mudstone.|
6057|Elgee Siltstone|61571|5|Briefly described|p656, p657 Fig. 4|Paleoproterozoic|Paleoproterozoic|Succession of siltstone and mudstone with sandstone intervals. Overlies Warton Sandstone;overlain by Pentecost Sandstone. Geological Province: Kimberley Basin.||||||07-NOV-08
6057|Elgee Siltstone|64104|6|Mentioned|p76 fig 10|Paleoproterozoic|Paleoproterozoic|||Unit in Kimberley Group.||||
6057|Elgee Siltstone|64580|4|Described|map legend||Paleoproterozoic|Of Kimberley Group. Siltstone, shale, stromatolitic dolomite, sandy dolomite, oolitic dolomite, and sandstone.||||||09-DEC-08
6057|Elgee Siltstone|64748|4|Described|p269 Fig 2, Tb.1, 271-275, 277-278|||Of Kimberley Group; Hematite bearing; sampled for palaeomag studies; of the Kimberley Group; Conformably underlies Pentecost Sandstone; overlies the Warton Sandstone; quartzose sandstone with siltstone and mudstone; ~40-480m thick; contains the Teronis Member; intruded by thin sills of Hart Dolerite||||||
6057|Elgee Siltstone|67563|6|Mentioned|p120, p122 Fig.2|||||Of the Kimberley Group.||||
6057|Elgee Siltstone|68078|6|Mentioned|p4 figure 2, p6 figure 3, p21 figure 14|Paleoproterozoic|Paleoproterozoic|Discontinued name||Kimberley Group||Overlies Warton Sandstone, Overlain by Pentecost Sandstone, intruded by Wotjulum Porphyry, Hart Dolerite|Siltstone.|
6057|Elgee Siltstone|68992|6|Mentioned|p498 Fig.1|||Kimberley Basin.||Of the Kimberley Group.||||
6057|Elgee Siltstone|69003|5|Briefly described|p20-21|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. Crops out along the Margaret River.||Kimberley Group.||Overlies Warton Sandstone. Is overlain by Pentecost Sandstone. Intruded by Wotjulum Porphyry.|Red-brown shale.|
6057|Elgee Siltstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. Unit relationships from geochron file 109639.1.pdf.||Kimberley Group|Includes Teronis Member|Underlies Pentecost Sandstone.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone|21-JUL-15
6057|Elgee Siltstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv.||Kimberley Group|Includes Teronis Member||Siltstone, shale and mudstone. Stromatolitic dolostone and dolomite, sandy dolostone, oolitic dolostone and sandstone.|
6057|Elgee Siltstone|69585|6|Mentioned|p3-5, p27|Statherian|Statherian|||Kimberley Group.||Conformably overlies Warton Sandstone.||
6057|Elgee Siltstone|69597|6|Mentioned|p4|||||||||
6057|Elgee Siltstone|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Minimum depositional age of 1740+\-6 Ma, based on magmatic crystallisation age of Wotjulum Porphyry that intrudes Elgee Siltstone. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1835-1740 Ma (Inferred)|Unit of Kimberley Group.|Includes Teronis Member.|Overlain by Pentecost Sandstone. Underlain by Warton Sandstone. Intruded by Wotjulum Porphyry.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone|
6057|Elgee Siltstone|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, Kimberley Craton.||Unit in Kimberley Group.|||Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin; North Australian Craton.||Kimberley Group.||Overlies Warton Sandstone. Is overlain by Pentecost Sandstone.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Upper Kimberley Group.||Overlies Buckland Point Member (Warton Sandstone). Is overlain by Pentecost Sandstone.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1740-1835 Ma|Kimberley Group|Includes Teronis Member||Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|70731|5|Briefly described|p270|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.||Unit of Kimberley Group.||||
6057|Elgee Siltstone|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.||Overlies Buckland Point Member (Warton Sandstone). Is overlain by Pentecost Sandstone.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.||Overlies Warton Sandstone. Is overlain by Pentecost Sandstone.  Intruded by Hart Dolerite.|Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|10-NOV-16
6057|Elgee Siltstone|71169|5|Briefly described|p82|Statherian|Statherian|Age of magnetization interpreted to be close to the depositional age (provided) of this unit.|c. 1790 Ma (Schmidt and Williams, 2008)|||||
6057|Elgee Siltstone|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological provice: Halls Creek Orogen; King Leopold Orogen. Of Kimberley Basin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv and geochron files.|1835-1740 Ma (inferred)|Unit of Kimberley Group.|Includes Teronis Member.|Overlain by Pentecost Sandstone. Underlain by Warton Sandstone. Intruded by Wotjulum Porphyry.|Massive red-brown siltstone with fine-grained micaceous, ferruginous and feldspathic sandstone interbeds; basal sequence in places of stromatolitic, sandy or oolitic dolomite, shale, micaceous siltstone and fine grained sandstone|
6057|Elgee Siltstone|71281|4|Described|p421, p423|Paleoproterozoic|Paleoproterozoic|Gellatly and Derrick (1967). Kimberley Basin. Up to 250m thick. Minimum age from intrusion.|> 1740 +/- 6 Ma.|Kimberley Group.||Overlies Warton Sandstone. Is overlain by Pentecost Sandstone. Is intruded by Wotjulum Porphyry.|Massive red-brown siltstone with thin, fine-grained micaceous, ferruginous and feldspathic sandstones; basal sequence can include stromatolitic, sandy or oolitic dolomite.|
6057|Elgee Siltstone|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.||Kimberley Group.|Teronis Member.|Overlies Warton Sandstone. Is overlain by Pentecost Sandstone.|Red-brown and grey siltstone, mudstone and sandstone; basal dolomitic siltstone that is locally oolitic and stromatolitic.|
6057|Elgee Siltstone|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.||Kimberley Group, upper|||Red-brown and grey siltstone and mudstone, stromatolitic dolostone, sandy dolostone, oolitic dolostone, and sandstone.|
6057|Elgee Siltstone|72437|6|Mentioned|p13|||||Kimberley Group||Intruded by the Wotjulum Porphyry.||
6057|Elgee Siltstone|72490|5|Briefly described|p3|||Maximum thickness of 250 m.||Kimberley Group|||Red-brown siltstone with thin interbeds of fine-grained micaceous, ferruginous and feldspathic sandstone. The basal interval includes beds of stromatolitic, sandy or oolitic dolomite.|
6061|Elimberrie Formation|42710|5|Briefly described|map legend|Proterozoic||Variation on Elimberrie Beds.||||||
6061|Elimberrie Formation|42811|4|Described|p29|Neoproterozoic|Neoproterozoic|Up to 1400 m thick. Diamictite towards top includes quartzite clasts with striations and percussion marks  (probable glacigene origin)||||Unconformably overlies Ellendale Formation. Other contacts faulted or sheraed.|Dolomitic limestone, dololutite, dolarenite, quartzite, feldspathic sandstone, siltstone & chert overlain by phyllite, quartzite, quartz sandstone, feldspathi sandstone, diamictite, thin ironstone interbeds.|17-OCT-12
6061|Elimberrie Formation|43281|5|Briefly described|Map legend||Proterozoic|||||||
6061|Elimberrie Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|neoproterozoic|Neoproterozoic||541-1000 Ma||||Sandstone, diamictite, siltstone, limestone, phyllite, quartzite, metabasalt, metatuff, and metarhyolite|
6061|Elimberrie Formation|71267|5|Briefly described|500k_interpgeop16_lut.csv|Neoproterozoic|Neoproterozoic|Of Oscar Range Sub-basin. Louisa Basin, Centralian Superbasin. Events: King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-541 Ma (inferred)||||Sandstone, diamictite, siltstone, limestone, phyllite, quartzite, metabasalt, metatuff, and metarhyolite|
6061|Elimberrie Formation|72034|6|Mentioned|500k_interpgeop16_lut|Neoproterozoic|Neoproterozoic|Informally grouped with Ninety Seven Mile Formation. Oscar Range Sub-basin, Louisa Basin.||||||
6075|Ellendale 11 Lamproite|41158|6|Mentioned|Table 38|||||||||
6077|Ellendale 2 Lamproite|41158|6|Mentioned|Table 34|||||||||
6078|Ellendale 23 Lamproite|41158|6|Mentioned|Table 40|||||||||
6079|Ellendale 31 Lamproite|41158|6|Mentioned|Table 40|||||||||
6080|Ellendale 38 Lamproite|41158|6|Mentioned|Table 40|||||||||
6082|Ellendale 7 Lamproite|41158|6|Mentioned|Table 36|||||||||
6084|Ellendale 9 Lamproite|41158|6|Mentioned|Table 37|||||||||
6087|Ellendale Formation|42710|5|Briefly described|map legend|Neoproterozoic|Mesoproterozoic|Variation on Ellendale Beds. 1864 m measured section.||Of Oscar Range Group||||17-OCT-12
6087|Ellendale Formation|42811|4|Described|p28|||Of Oscar Range Group.||||Overlies Le Lievre Formation. Contact unconformable to faulted.|1464m of cobble and boulder conglomerate, quartzite, quartz sandstone, feldspathic sandstone and siltstone, overlain by 400m of laminated siltstone.|17-OCT-12
6087|Ellendale Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Oscar Range Group.|||Cross bedded and rippled grey-green to brown phyllitic sandstone, feldspathic sandstone and minor siltstone and cobble and boulder conglomerate, overlain by laminated siltstone with occasional hematite lenses|
6108|Ellis Sandstone|22804|6|Mentioned|Fig 2 on p432|Neoproterozoic|Neoproterozoic|||||||
6108|Ellis Sandstone|22826|6|Mentioned|Fig 2 on p565|Neoproterozoic|Neoproterozoic|||||||
6108|Ellis Sandstone|24301|6|Mentioned|p17|||||||||
6108|Ellis Sandstone|31914|6|Mentioned|p96|||U.Proterozoic||||||
6108|Ellis Sandstone|33588|6|Mentioned|p6|||||||||
6108|Ellis Sandstone|34442|6|Mentioned|p8|||Equiv. Pertatataka Formation||||||
6108|Ellis Sandstone|35102|6|Mentioned|Fig.2|||||||||
6108|Ellis Sandstone|35127|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6108|Ellis Sandstone|35222|4|Described|Table.2|||||||||
6108|Ellis Sandstone|35863|6|Mentioned|Table 1|||||||||
6108|Ellis Sandstone|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6108|Ellis Sandstone|36551|6|Mentioned|Table 13|||||||||
6108|Ellis Sandstone|36887|5|Briefly described|p211|||||||||
6108|Ellis Sandstone|37928|6|Mentioned|Fig.4|||||||||
6108|Ellis Sandstone|40740|6|Mentioned|p1|||||||||
6108|Ellis Sandstone|41852|6|Mentioned|p209|||||||||
6108|Ellis Sandstone|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, siltstone, conglomeratic sandstone.  Geological province: Amadeus Basin.||||||23-JAN-08
6108|Ellis Sandstone|43503|6|Mentioned|50|||||||||
6108|Ellis Sandstone|44395|14|Not recorded|p.6,12, Tb.1||Proterozoic|Correlates with Winnall Beds and Pertatataka Formation.||||||
6108|Ellis Sandstone|44396|5|Briefly described|map legend|||(Proterozoic-Lower Palaeozoic). First Edition. SF/52-15.||||||
6108|Ellis Sandstone|44439|2|Defined|p.7,8, Tb.1, map|Cambrian|Neoproterozoic|U.Prot.-Cambrian. Laterally equiv.to Sir Frederick Conglomerate. Both probably equiv.to Mt.Currie Conglomerate on G52-3 (Bloods Range N.T.).||||||
6108|Ellis Sandstone|44440|14|Not recorded|map legend|Cambrian|Neoproterozoic|Upper Proterozoic-Cambrian.||||||
6108|Ellis Sandstone|44499|14|Not recorded|opp.p.6, Tb.1|||Proterozoic to Lower Palaeozoic?||||||
6108|Ellis Sandstone|44500|5|Briefly described|map legend|||Proterozoic to Lower Palaeozoic?||||||
6108|Ellis Sandstone|45041|4|Described|p38|||Equiv. Winnall Beds||||||
6108|Ellis Sandstone|45149|6|Mentioned|Table 1|||Page 17.||||||
6108|Ellis Sandstone|48842|2|Defined|p.17,18|Early Paleozoic|Neoproterozoic|p.8,14,15,17,18,19,22,23,27,Pl.5,7,8. Tb.I. (new name). Overlies Carnegie or Boord Fms. Interfingers with Sir Frederick Cong; Overlain by Maurice Fm. Upper Proterozoic-Lower Palaeozoic.||||||07-NOV-08
6108|Ellis Sandstone|48864|14|Not recorded|Tb.1,p.10,28,Pl.10|||Cambrian? (G52-2).||||||
6108|Ellis Sandstone|48963|6|Mentioned|Fig.2|||||||||
6108|Ellis Sandstone|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Kaolinitic quartz sandstone; minor calcareous sandstone and siltstone.  Geological Province: Amadeus Basin.||||||
6108|Ellis Sandstone|61387|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Kaolinitic quartz sandstone; minor calcareous sandstone and siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
6108|Ellis Sandstone|61519|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Kaolinitic, quartz sandstone; minor calcareous sandstone and siltstone. Geological Province: Amadeus Basin.||||||
6108|Ellis Sandstone|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
6108|Ellis Sandstone|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||
6108|Ellis Sandstone|62609|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, siltstone, conglomeratic sandstone. Underlies: Maurice Formation. Overlies: Carnegie Formation.||||||14-AUG-06
6108|Ellis Sandstone|62620|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Sandstone, siltstone, conglomeratic sandstone.||||||
6108|Ellis Sandstone|64580|4|Described|map legend||Neoproterozoic|Sandstone, quartz wacke, and siltstone.||||||09-DEC-08
6108|Ellis Sandstone|64809|6|Mentioned|p3 Fig.2 |Proterozoic|Proterozoic|||||||
6108|Ellis Sandstone|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
6108|Ellis Sandstone|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
6108|Ellis Sandstone|65256|6|Mentioned|p19|||Stratigraphic correlative of the Winnall beds.||||||
6108|Ellis Sandstone|67326|5|Briefly described|p2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Is overlain by Maurice Formation and Winnall beds.||
6108|Ellis Sandstone|67856|4|Described|p340, p338, 335, 337, 339, 344, 345|Neoproterozoic|Neoproterozoic|Of Wells et al., 1964, 1970. Type section: not designated. No age determination. 610m thick.||||Unconformably overlain by Maurice Formation. Interfingers with + equivalent to Ellis Sandstone, equivalent to Winnall beds. Unconformably overlies Carnegie, Boord, Bitter Springs Formations.|Cross-bedded quartz, kaolinitic and pebbly sandstone; some interbedded calcareous sandstone and siltstone; clay pellets; heavy mineral concentration.|
6108|Ellis Sandstone|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by Mount Currie Conglomerate. Underlain by Boord Formation.||
6108|Ellis Sandstone|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
6108|Ellis Sandstone|69003|6|Mentioned|p60|Cambrian|Cambrian|W Amadeus Basin.||||||
6108|Ellis Sandstone|69031|5|Briefly described|p4, p9|||Amadeus Basin. Deposited during the c.580-530 Ma Petermann Orogeny.||||Overlies Carnegie Formation. Is overlain by Maurice Formation.||
6108|Ellis Sandstone|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Is overlain by Maurice Formation.||12-JUL-16
6108|Ellis Sandstone|69438|4|Described|p23:2-4, 18, 20-21, 23|Early Cambrian|Ediacaran|Wells et al. (1965). Amadeus Basin. A correlative of lower Winnall beds and middle Arumbera Sandstone.||Pertaoorrta Group.||Conformably overlies Carnegie and Boord Formations. Interfingers with Sir Frederick Conglomerate. Is overlain conformably by Maurice Formation.|Cross-bedded kaolinitic quartz sandstone and pebbly sandstone, with subordinate calcareous sandstone and siltstone; cross-beds indicate sediment was sourced from the W and SW.|12-JUL-16
6108|Ellis Sandstone|69606|4|Described|p1, p3, p4 fig 2, p6 fig 3, p7 fig 4|Early Cambrian|Late Ediacaran|Deposited during the Petermann Orogeny. Potential source and reservoir rock. No type section has been nominated. Forms prominent strike ridges with an average thickness of 500m. Interpreted to be of fluvial origin. See also  p14, p16, p17, p18.||||(apparently conformably) Overlies the Carnegie Formation, overlain by the Maurice Formation. Inferred to interfinger with the Sir Frederick Conglomerate. Correlated with the Winnall beds.|Pale  brown to pale purple medium grained sandstone, commonly with an orange-brown weathering skin. Trough and tabular cross-bedding and current lineations are common, as are mud pellets in some areas.|
6108|Ellis Sandstone|69673|6|Mentioned|p64 fig 53, p65, p88, p91|||Potential reservoir rock,||||Overlies Carnegie Formation, overlain by Maurice Formation||
6108|Ellis Sandstone|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Winnall Group.||Overlies Carnegie Formation. Is overlain by Maurice Formation.||
6108|Ellis Sandstone|70826|6|Mentioned|p5 tbl 2|||Supersequence 4, Centralian Superbasin.||||||20-APR-20
6108|Ellis Sandstone|70839|4|Described|p329-333,335,337-340|Ediacaran|Ediacaran|Of Amadeus Basin. Part of Supersequence 4. Ridge-forming unit typically around 500m thick. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Concordant dates range between c. 0.97 and c. 1.9 Ga. Dominant age component between c. 1.22 and c. 1.04 Ga,with minor components at c. 1.3, 1.5, 1.6 and 1.7 Ga.|Max dep age: 967+\-11 Ma (238U/206Pb)|||Overlain by Maurice Formation. Underlain by Carnegie Formation. Equivalent to Sir Frederick Conglomerate. Correlable to unit 2 of the Winnall beds.|Fluvial pebbly sandstone.|
6108|Ellis Sandstone|71080|5|Briefly described|p30 fig 21|Cambrian||Amadeus Basin in WA. Supersequence 4.|||||Dominantly sandstone.|
6108|Ellis Sandstone|71088|4|Described|p1-p2, p7-p8, p12, p15-p17, p19-p21, p24|early Cambrian|Late Ediacaran|Amadeus Basin. Reassigned to Supersequence 4. Potentially equivalent to the Sir Frederick Conglomerate. Correlated with the Pertatataka Formation by Wells et al., 1970; Grey, 1990 and Lindsay and Korsch., 1991. Sedimentary structures include trough and tabular cross-bedding and current lineations. Inferred to have been deposited in a fluvial environment in WA and a likely deltaic environment in the NT. This formation is typically about 500m thick but thins northwards. Previously correlated with the Pertatataka Formation, this has been rejected in the present study in favour of correlation with the Arumbera Sandstone. No biostratigraphic evidence has been found in WA but on the basis of itys correlation its age could range from late Ediacaran to early Cambrian.||||Overlies (potentially disconformably) the Carnegie Formation. Overlain by the Maurice Formation. Equivalent to the Winnall beds and Arumbera Sandstone.|Pale-brown, pebbly, medium-grained feldspathic sandstone.|02-MAY-23
6108|Ellis Sandstone|71114|5|Briefly described|p170 fig 1b|Terreneuvian|Ediacaran|SW Amadeus Basin.||||Shown as lateral equivalent to Sir Frederick Conglomerate, Mount Currie Conglomerate.||14-FEB-18
6108|Ellis Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
6108|Ellis Sandstone|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Cross-bedded quartz sandstone and pebbly sandstone; may be kaolinitic; minor interbedded calcareous sandstone and siltstone.|
6108|Ellis Sandstone|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Ediacaran|Amadeus Basin.||Pertaoorrta Group.||||
6108|Ellis Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1055+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Fine- to coarse-grained lithic quartz sandstone.|
6108|Ellis Sandstone|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Carnegie Formation. Overlain by the Maurice Formation.|Lithic sandstone.|
6108|Ellis Sandstone|71810|5|Briefly described|Map legend.|Cambrian|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.||||Overlies Carnegie Formation. Is overlain by Maurice Formation.|Medium-grained, cross-bedded, white to pale brown sandstone and pebbly sandstone (inferred to have been deposited during the Petermann Orogeny).|
6108|Ellis Sandstone|71841|5|Briefly described|p1|Early Cambrian|Ediacaran|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Sir Frederick or Mount Currie conglomerates.||
6108|Ellis Sandstone|71842|4|Described|iii,p2-3,5,7-9|Early Cambrian|Ediacaran|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA).||Unit of Pertaoorrta Group.||Overlain by Maurice Formation. Underlain by Carnegie Formation. Grades into Sir Frederick Conglomerate. Correlable to Arumbera Sandstone or Winnall beds.|Poorly sorted, clean, cross-bedded, silicified, quartz sandstone with variable bed thickness, numerous lenses of conglomerate comprised of quartzite and black chert clasts.|
6108|Ellis Sandstone|72358|6|Mentioned|p118|Series 1|Ediacaran|Of Amadeus Basin.||||||
6108|Ellis Sandstone|72360|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.|||||Kaolinitic quartz sandstone; minor calcareous sandstone and siltstone.|09-SEP-19
6108|Ellis Sandstone|72601|6|Mentioned|p3, p11-12, p14|Cambrian|Ediacaran|Amadeus Basin, western portion[?]. Previously mapped together with the Carnegie Formation as the Winnall beds.||||||
6117|Elvire Formation|22496|4|Described|p11||Neoproterozoic|Of the Albert Edward Group.  Mainly maroon to grey siltstone.  Overlies Mount Forster Sandstone.  Geological Province:  Wolfe Basin.||||||16-AUG-04
6117|Elvire Formation|22547|6|Mentioned|p28||Neoproterozoic III|Of the Albert Edward Group.||||||14-NOV-06
6117|Elvire Formation|22649|6|Mentioned|p 141|||Rb-Sr isotope age 639+/-47 Ma  p141.  Kimberley Region.||||||
6117|Elvire Formation|22777|5|Briefly described|Map|||Albert Edward Group, Wolfe Basin||||||
6117|Elvire Formation|23621|4|Described|p34|Neoproterozoic|Neoproterozoic|See also page 9 table 1. Of Albert Edward Group. Overlying unit Boonall Dolomite. Underlying unit Mount Forster Sandstone. Wolfe Basin. Max. thickness: 100 m.||||||
6117|Elvire Formation|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Albert Edward Group. Geological Province: Wolfe Basin.||||||
6117|Elvire Formation|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Albert Edward Group.||||||
6117|Elvire Formation|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Albert Edward Group. Friable maroon to brown siltstone/shale. Overlain by Boonall Dolomite; underlain by Mount Forster Sandstone. Geological Province: Wolfe Basin. Max Thickness: <100m.||||||06-APR-05
6117|Elvire Formation|29813|4|Described|Table 2|||||||||
6117|Elvire Formation|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6117|Elvire Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6117|Elvire Formation|32109|6|Mentioned|Table 1|||Precambrian||||||
6117|Elvire Formation|32660|5|Briefly described|Table 6|||||||||
6117|Elvire Formation|32728|6|Mentioned|Fig.16|||See also Table 7||||||
6117|Elvire Formation|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6117|Elvire Formation|36551|6|Mentioned|Table 12|||||||||
6117|Elvire Formation|36888|4|Described|p214|||||||||
6117|Elvire Formation|36898|5|Briefly described|Table II|||See also p181.||||||05-SEP-18
6117|Elvire Formation|37462|6|Mentioned|p294|||||||||
6117|Elvire Formation|37927|6|Mentioned|p511|||||||||
6117|Elvire Formation|38157|6|Mentioned|Table X|||||||||
6117|Elvire Formation|39210|5|Briefly described|p49|||||||||
6117|Elvire Formation|41429|6|Mentioned|p247|||||||||
6117|Elvire Formation|43299|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
6117|Elvire Formation|43303|5|Briefly described|Map Legend||Neoproterozoic|of Albert Edward Group.||||||
6117|Elvire Formation|43855|5|Briefly described|Map Legend||Proterozoic|||||||
6117|Elvire Formation|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Osmond Range (East Kimberley) area. 61 m thick.||Of Albert Edward Group.||Conformably overlies Mount Forster Sandstone. Overlain conformably by Boonall Dolomite.|Red-brown shale with green siltstone; minor sandstone.|07-MAR-18
6117|Elvire Formation|44317|4|Described|Table 3 p.7||Adelaidean|||||||
6117|Elvire Formation|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
6117|Elvire Formation|44324|14|Not recorded|p.10||Adelaidean|Tb.2. (Adelaidean) of Albert Edward Group.||||||
6117|Elvire Formation|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
6117|Elvire Formation|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
6117|Elvire Formation|45047|2|Defined|p95|Adelaidean|Adelaidean|See p36.||||||18-MAY-15
6117|Elvire Formation|45140|3|Fully described|p13, p59, Appx.p36-37|||Dow and Gemuts (1969). Named after Elvire River. Unnamed basin NW of Birrindudu Basin. 390m thick. No fossils known.||Albert Edward Group.||Conformably overlies Mount Forster Sandstone. Is overlain conformably by Timperley Shale or, where present, Boonall Dolomite.|Medium- to fine-grained lithic arenite, thinly interbedded siltstone and shale.|
6117|Elvire Formation|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Albert Edward Group. Geological Province: Wolfe Creek Basin. Thin bedded argillite; minor quartz sandstone.||||||
6117|Elvire Formation|63458|6|Mentioned|p884; p886,p889,p897 Figs.11,14,19. |Ediacaran|Ediacaran|||Unit in Albert Edward Group.||Is overlain conformably by Boonall Dolomite.|Mudstone.|
6117|Elvire Formation|64104|6|Mentioned|p62 fig.1, p73 Tb.3, p74. |Neoproterozoic|Neoproterozoic|||Unit in Albert Edward Group.||Overlies Mount Forster Sandstone. Is overlain by Boonall Dolomite.||
6117|Elvire Formation|67484|6|Mentioned|p294, p295 Fig.2|Ediacaran|Ediacaran|East Kimberley.||Of the Albert Edward Group.||Overlain by the Boonall Dolomite. Underlain by the Mount Forster Sandstone.||
6117|Elvire Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|East Kimberley region.||Albert Edward Group.||Overlies Mount Forster Sandstone. Is overlain by Boonall Dolomite.||
6117|Elvire Formation|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Albert Edward Group.||||
6117|Elvire Formation|68244|4|Described|p660,p666-667|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region. Glaciogenic unit deposited during of Egan Glaciation.||Unit of Albert Edward Group.||Overlain by Boonall Dolomite. Underlain by Mount Forster Sandstone.||21-JUN-19
6117|Elvire Formation|68473|6|Mentioned|p531|||||||||
6117|Elvire Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Of Albert Edward Group.|||Thin-bedded siltstone and mudstone; minor quartz sandstone.|31-JUL-15
6117|Elvire Formation|69165|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||||||Thin-bedded siltstone and mudstone; minor quartz sandstone.|
6117|Elvire Formation|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Albert Edward Group.|||Thin-bedded siltstone and mudstone; minor quartz sandstone|
6117|Elvire Formation|70154|6|Mentioned|100k_interpgeop_lut.csv|Fortunian|Ediacaran||541-635 Ma|Albert Edward Group||||
6117|Elvire Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv,  1M_geologyp12_lut.csv.|635-541 Ma (inferred)|Unit of Albert Edward Group.|||Thinly bedded to laminated, partly micaceous, red-brown shale and green siltstone with minor thinly bedded lithic and quartzose sandstone mainly near the top and bottom|
6117|Elvire Formation|73255|6|Mentioned|p534 Fig.2|Ediacaran|Ediacaran|||Albert Edward Group||Overlies the Mount Forster Sandstone, underlies the Boonall Dolomite.||
6150|Empress Formation|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
6150|Empress Formation|34829|6|Mentioned|Fig.2|||||||||
6150|Empress Formation|37373|6|Mentioned|Tab 2.VII|||||||||
6150|Empress Formation|44150|6|Mentioned|p133 Tb.2-16|||West Pilbara. Of Fitton et al. (1975). Probably obsolete? Apparently subsequently divided into Apex Basalt, Panorama Formation and Euro Basalt. ||||Equivalent to Miralga Formation in East Pilbara.||
6177|Enderby Formation|24390|5|Briefly described|p24 Table 6|||Geological Province: Northern Carnarvon Basin.||||||
6177|Enderby Formation|29721|6|Mentioned|p102|||||||||
6177|Enderby Formation|31604|6|Mentioned|p6|||Liassic. Unit of Dingo Gp. Table 4.||||||
6177|Enderby Formation|32711|6|Mentioned|Fig.3|||||||||
6177|Enderby Formation|32714|6|Mentioned|Fig.7|||Jurassic. Dingo Gp.||||||
6177|Enderby Formation|32715|6|Mentioned|Fig.16|||||||||
6177|Enderby Formation|50085|5|Briefly described|p24 Tb. 6|Middle Jurassic|Middle Jurassic|Name appears as Enderby Fms. in text of Table.  Geological Province: Northern Carnarvon Basin.||||||
6185|Enga Sandstone|13194|4|Described|p390 Tb. 4-16, p402 fig 4-66|Middle Tournaisian|Middle Tournaisian|Type Section: Enga Ridge 15o49'S 128o56'E. 160-320m thick barrier complex and shoreface deposits.||Langfield Group||Overlies Burt Range Formation (conformably). Overlain by Septimus Limestone (conformably).|Sandstone with minor siltstone, shale and sandy limestone.|
6185|Enga Sandstone|13234|5|Briefly described|p252, p260 Tb.1.|Early Carboniferous|Early Carboniferous|Includes traces of oil. Proven reservoir.||||||27-OCT-14
6185|Enga Sandstone|23820|5|Briefly described|p202 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Gulf Basin.||||||
6185|Enga Sandstone|32648|6|Mentioned|p32|||Tournaisian||||||
6185|Enga Sandstone|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
6185|Enga Sandstone|32699|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Calcareous quartz sandstone.||||||02-DEC-04
6185|Enga Sandstone|32701|4|Described|Table 2|||L.Carb. See also p16.||||||15-AUG-06
6185|Enga Sandstone|32867|6|Mentioned|p27|||||||||
6185|Enga Sandstone|32870|5|Briefly described|p46|||||||||
6185|Enga Sandstone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
6185|Enga Sandstone|36257|6|Mentioned|Table 2.1|||||||||
6185|Enga Sandstone|36473|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
6185|Enga Sandstone|36551|6|Mentioned|Table 16|||||||||
6185|Enga Sandstone|36890|3|Fully described|p379|||||||||
6185|Enga Sandstone|36904|5|Briefly described|p9|||See also p12.||||||15-AUG-06
6185|Enga Sandstone|39827|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
6185|Enga Sandstone|40494|4|Described|p17|||Also mention on p14.||||||15-AUG-06
6185|Enga Sandstone|40792|6|Mentioned|p175|||||||||
6185|Enga Sandstone|40993|6|Mentioned|p10|||||||||
6185|Enga Sandstone|41598|6|Mentioned|p412|||||||||
6185|Enga Sandstone|41712|6|Mentioned|p285|||||||||
6185|Enga Sandstone|41731|6|Mentioned|p519|||||||||
6185|Enga Sandstone|41839|4|Described|p28|||||||||
6185|Enga Sandstone|41864|2|Defined|p105|||See also Fig.108. Formerly called "Snowie Sandstone".||||||15-AUG-06
6185|Enga Sandstone|41865|5|Briefly described|Map legend||Tournaisian|||||||
6185|Enga Sandstone|42442|6|Mentioned|p11|||||||||
6185|Enga Sandstone|42547|4|Described|p98|||||||||
6185|Enga Sandstone|42829|6|Mentioned|Fig.5 P146|||||||||
6185|Enga Sandstone|42994|6|Mentioned|p65|||||||||
6185|Enga Sandstone|44965|14|Not recorded|Not recorded|||||||||
6185|Enga Sandstone|44993|14|Not recorded|p.15|||||||||
6185|Enga Sandstone|44994|6|Mentioned|p14|||Tournaisian. Correlation Fig.6.||||||
6185|Enga Sandstone|44998|14|Not recorded|App.3 p277,279|||Overlain by Septimus Limestone.||||||
6185|Enga Sandstone|45038|14|Not recorded|p.79|||||||||
6185|Enga Sandstone|45039|6|Mentioned|p1|||See also PP6,7,8 etc. Lower Carboniferous.||||||
6185|Enga Sandstone|45050|6|Mentioned|Table 2|||See also Table 4 & PP5,7,12,33||||||
6185|Enga Sandstone|45063|6|Mentioned|p8|||Tournaisian. See also P17, 25 & Fig. 3||||||
6185|Enga Sandstone|45097|6|Mentioned|Fig.|||Correlation chart||||||
6185|Enga Sandstone|45133|6|Mentioned|p4|||||||||
6185|Enga Sandstone|45169|4|Described|p4|||||||||
6185|Enga Sandstone|48635|14|Not recorded|Fig.1||Early Carboniferous|(D/52-10,11,14,15). Lower Carboniferous.||||||
6185|Enga Sandstone|48831|14|Not recorded|p.60|||||||||
6185|Enga Sandstone|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
6185|Enga Sandstone|60006|5|Briefly described|Map Legend|Tournaisian|Tournaisian|Geological Province: Bonaparte Basin. Of Langfield Group. Calcareous quartz sandstone, siltstone, shale, quartzic limestone.||||||22-JUL-04
6185|Enga Sandstone|60364|4|Described|p184, 187, 194|Tournaisian|Tournaisian|Conformably overlies Burt Range Formation. Conformably overlain by Septimus Limestone. Thickness: 160 m. Clean, well sorted medium-grained quartz sandstone with minor calcarenite interbedded near base. Fossiliferous. Of Langfield Group.||||||
6185|Enga Sandstone|60682|4|Described|piii, 22, Table 5, 24|Tournaisian|Tournaisian|Of Langfield Group. Conformably overlies Burt Range Formation. Conformably overlain by Septimus Limestone. Max. thickness: <150m. Geological Province: Bonaparte Basin. Quartz sandstone, siltstone, shale and quartzitic limestone.||||||
6185|Enga Sandstone|61542|5|Briefly described|p277 Fig. 2|Tournaisian|Tournaisian|Of the Langfield Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
6185|Enga Sandstone|64580|6|Mentioned|map legend|||Of Langfield Group.||||||15-DEC-08
6185|Enga Sandstone|64694|5|Briefly described|p234 Fig.2, p235, p253, p254 Fig.12|Tournaisian|Tournaisian|Burt Range Shelf, Onshore Bonaparte Basin.||Unit in Langfield Group.||Overlies Burt Range Formation. Is overlain by Septimus Limestone.|Dolomitic sandstone.|
6185|Enga Sandstone|65331|5|Briefly described|Map legend|Tournasian|Tournasian|Of Langfield Group, Bonaparte Basin. Calcareous quartz sandstone, siltstone, shale, quartzic limestone ||||||
6185|Enga Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||31-JUL-15
6185|Enga Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Langfield Group||||
6185|Enga Sandstone|69452|4|Described|p36:6, 9, 12-13, 28|Tournaisian|Tournaisian|Traves (1955); equivalent to "Snowie Sandstone" of Traves (1949). Petrel Sub-basin, Bonaparte Basin. Shallow-marine, tidal channel, barrier/lagoon, beach deposits. Up to 320m thick in WA; less than 150m in NT. Onshore. Has produced dry gas flows in most cases where it is intersected.||Langfield Group.||Conformably (locally unconformably) overlies Burt Range Formation. Is overlain conformably by Septimus Limestone. Is faulted against Kellys Knob Sandstone and Border Creek Formation.|Quartz sandstone, minor siltstone, shale and quartzose limestone. Beds range from massive to laminated to cross-bedded, and may be bioturbated. Diverse fossil assemblage.|12-JUL-16
6185|Enga Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Tournaisian|||Unit of Langfield Group.||||
6185|Enga Sandstone|69673|5|Briefly described|viii, p166, p171, p179, p180|Tournaisian|Late Devonian|Proven gas reservoir.||Langfield Group|||Fossiliferous quartz sandstone with minor siltstone, shale and quartzic limestone.|
6185|Enga Sandstone|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin.||Langfield Group|||Calcareous quartz sandstone, siltstone, shale, quartzic limestone.|
6185|Enga Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Well sorted, medium-grained quartz sandstone, calcareous in part, siltstone, shale, quartzic limestone; fossiliferous|
6199|Enokurra Sandstone|34203|6|Mentioned|p15|||||||||
6199|Enokurra Sandstone|36293|2|Defined|p57|Proterozoic|Proterozoic|||||||
6199|Enokurra Sandstone|36872|3|Fully described|p73|||||||||
6199|Enokurra Sandstone|37460|6|Mentioned|p178|||||||||
6199|Enokurra Sandstone|40307|6|Mentioned|Fig.2|||||||||
6199|Enokurra Sandstone|40346|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6199|Enokurra Sandstone|40347|6|Mentioned|p16|||||||||
6229|Erica Sandstone|22496|6|Mentioned|p10||Neoproterozoic|Redcliff Pound Group||||||
6229|Erica Sandstone|29806|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6229|Erica Sandstone|29807|4|Described|Table 1|||See also p16.||||||16-AUG-06
6229|Erica Sandstone|29809|6|Mentioned|Table 1|||||||||
6229|Erica Sandstone|29810|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6229|Erica Sandstone|29813|4|Described|Table 2|||||||||
6229|Erica Sandstone|29817|6|Mentioned|p7|||||||||
6229|Erica Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6229|Erica Sandstone|29819|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6229|Erica Sandstone|31360|4|Described|Table 1|||||||||
6229|Erica Sandstone|35205|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6229|Erica Sandstone|35222|6|Mentioned|p10|||||||||
6229|Erica Sandstone|36532|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6229|Erica Sandstone|36551|6|Mentioned|Table 12|||||||||
6229|Erica Sandstone|45140|2|Defined|p13, p40, p44, p48-52, p56, p58 Fig.43|||See also Appx.p26-28. Blake and Yeates (1977), Crowe and Muhling (1977). Widespread unit. Named after the Erica Range. Birrindudu Basin. Previously mapped partly as Phillipson Beds and partly as Gardiner Beds (Wells, 1962; Casey and Wells, 1964). Up to 700m thick. Forms cuestas, plateaus, strike ridges and hills up to 60m high. The type section is 400m thick across the main cuesta of the Erica Range, from 21deg 05'50"S, 128deg 30'00"E to 21deg 07'00"S, 128deg 29'00"E. A representative section is also described in some detail. Is broadly folded and gently dipping. Surface silicification widespread, local laterite cappings. Probably equivalent to Boee Beds. Faulted against Baines Beds.||Topmost Redcliff Pound Group.||Conformably overlies Murraba Formation. Is overlain ?unconformably by Lucas Formation, Pedestal and Hazlett Beds; and ?conformably by Hidden Basin Beds (also faulted against it).|Mainly well-sorted, medium- to fine-grained friable sublithic arenite; mainly medium-bedded, white or purple to reddish-brown. Also medium-grained quartz arenite, thin-bedded to laminated shale, siltstone, fine-grained arenite, glauconitic sandstone.|
6229|Erica Sandstone|46864|4|Described|p38|||||||||
6229|Erica Sandstone|62632|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Redcliff Pound Group. Geological Province: Murraba Basin. Well sorted medium to fine grained, sublithic sandstone with silica cement, crossbedded, ripple, minor conglomerate.||||||23-DEC-09
6229|Erica Sandstone|65074|4|Described|p351 fig 4-37, p353, p356 Tb. 4-12, p358|Neoproterozoic|Neoproterozoic|Of Birrindudu Basin. 700m thick. Type section is in Erica Range; details given.||Redcliff Pound Group||Conformably overlies Murraba Formation. Equivalent to Boee beds. Is overlain by Hidden Basin beds.|Medium- to fine-grained sublithic arenite with glauconitic sandstone near the top.|
6229|Erica Sandstone|67163|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Unit in Redcliff Pound Group.||Overlies Murraba Formation and Munya Sandstone.|Well-sorted, medium- to fine-grained sublithic sandstone with silica cement, crossbedded, ripples; minor conglomerate.|
6229|Erica Sandstone|69288|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin.||Redcliff Pound Group.|||Well-sorted, medium- to fine-grained, sublithic sandstone with silica cement, cross-bedded, ripples; minor conglomerate.|
6229|Erica Sandstone|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|Murraba Basin, Centralian A Superbasin. Supersequence 1.||Redcliff Pound Group.||Overlies Murraba Formation.||12-JUL-16
6229|Erica Sandstone|69440|4|Described|p25:1-2|Cryogenian|Cryogenian|Murraba Basin. Occurs in western HIGHLAND ROCKS map area where it is c.50m thick. Maximum thickness of 700m in WA where it is most extensively exposed. Fluvial to partly shallow-marine deposition. May be overlain conformably by Hidden Basin beds, but the contact is hidden or faulted.||Redcliff Pound Group.||Conformably overlies Murraba Formation. Correlates with Boee beds (WA). Is overlain unconformably by Lucas Formation and Pedestal beds.|Predominantly well-sorted, medium to fine sublithic sandstone with up to 10% clay matrix; some glauconitic sandstone.|12-JUL-16
6229|Erica Sandstone|69673|5|Briefly described|p187|||50m thick.||Redcliff Pound Group||Conformably overlies Murraba Formation|Sublithic sandstone and some glauconitic sandstone.|
6229|Erica Sandstone|70130|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||Redcliff Pound Group.||Overlies Murraba Formation.|Lithic sandstone and quartz sandstone.|
6229|Erica Sandstone|71080|4|Described|p11, 14-18, 27,28, 29, 32, 36-37|Cambrian|Ediacaran|Murraba Basin. 400m thick in type section in Erica Range, but no boundaries seen here. Named after the Erica Range, largely restricted to LUCAS and STANSMORE map sheets in WA and HIGHLAND ROCKS in the NT.Definition needs revision. Picking boundary with underlying Murraba Formation is problematic. Change from shallow-marine to deltaic depositional environment should be considered correlative across basin. See also p4, 5, 7.||Redcliff Pound Group||Considered conformable on underlying Murraba Formation where contact seen. Unconformably overlain by Palaeozoic outliers of Canning Basin. Inferred to be overlain by Antrim Plateau Volcanics in NT.|Predominantly well-sorted, fine- to medium-grained, friable, sublithic arenite that has up to 10% clay matrix. Mainly medium bedded and either white or iron stained to purple or reddish-brown. Cross-bedding is very common.|04-FEB-19
6229|Erica Sandstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Redcliff Pound Group.|||Shallow marine, well sorted, mainly fine to medium grained, sublithic and minor quartz sandstone, siltstone, shale and glauconitic sandstone; cross bedded, ripples; minor conglomerate|
6229|Erica Sandstone|73445|5|Briefly described|p7, 10, 12-14|Cambrian||Whole-rock chemistry tabulated. The boundary with Murraba Formation is time-transgressive.||Redcliff Pound Group.||Overlies Murraba Formation.|Quartz-rich sandstone; siliciclastic sedimentary rocks.|
6243|Errabiddy Sandstone|23569|6|Mentioned|p7|Proterozoic|Proterozoic|Superseded by Errabiddy Formation||||||
6243|Errabiddy Sandstone|38493|6|Mentioned|p33|||||||||
6243|Errabiddy Sandstone|38494|4|Described|p26|||||||||
6243|Errabiddy Sandstone|40336|4|Described|p15|||||||||
6243|Errabiddy Sandstone|40339|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
6243|Errabiddy Sandstone|43255|5|Briefly described|map legend||Proterozoic|of Badgeradda Group.||||||
6243|Errabiddy Sandstone|43256|6|Mentioned|17||Proterozoic|of Badgeradda Group||||||
6243|Errabiddy Sandstone|44142|5|Briefly described|p328 Tb.4-5|||In Mowry Hill area, bounded by Meeberrie Fault to west. Overlies Western Gneiss Terrane.||Badgeradda Group||Correlated with Bangemall Group.|Fine- to coarse-grained sandstone, pebbly sandstone; feldspathic sandstone, pebbly conglomerate.|
6243|Errabiddy Sandstone|45015|5|Briefly described|p22, map legend|Proterozoic|Proterozoic|Of Badgeradda Group.  Lithologically similar to Woodrarrung Sandstone, but not continuous with it. Structure suggests may be equivalent to part of Coomberarie Formation of Badgeradda Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
6243|Errabiddy Sandstone|48823|5|Briefly described|p3 Tb. 1, p13, map legend|Mesoproterozoic|Mesoproterozoic|Of the Badgeradda Group.  Medium- to coarse-grained feldspathic sandstone. Thickness: 480ft.||||||
6243|Errabiddy Sandstone|61958|5|Briefly described|Map sheet 1|Neoproterozoic|Neoproterozoic|Of the Badgeradda Group.||||||21-MAR-06
6243|Errabiddy Sandstone|64580|4|Described|map legend||Mesoproterozoic|Of Badgeradda Group. Feldspathic sandstone; minor pebble conglomerate lenses.||||||09-DEC-08
6243|Errabiddy Sandstone|69028|5|Briefly described|Map Legend|Stenian|Stenian|Badgeradda Basin.|c. 1055 Ma||||Feldspathic sandstone; minor pebble conglomerate lenses.|06-MAY-14
6243|Errabiddy Sandstone|69166|5|Briefly described|500k_geologyp08_lut.csv|Mesoproterozoic|Mesoproterozoic|||Badgeradda Group|||Feldspathic sandstone; minor pebble conglomerate lenses.|
6243|Errabiddy Sandstone|72259|6|Mentioned|p3|Stenian|Stenian||ca. 1055 Ma|||||
6256|Erskine Sandstone|7433|5|Briefly described|p25 Fig.2, pp40-41, p52.|Triassic|Triassic|Gregory and Fitzroy Sub-basins, Canning Basin. Fine deltaic clastics. Excellent aquifer potential.||||Overlies Blina Shale.|Fine sandstone, siltstone. Minor patchy white to grey silcrete developed along joint intersections.|
6256|Erskine Sandstone|13354|6|Mentioned|p376 Fig.7.|Middle Triassic|Early Triassic|Onshore Canning Basin. Overlies Blina Shale.||44||||28-OCT-14
6256|Erskine Sandstone|22753|5|Briefly described|Fig.3 p585|Triassic|Triassic|||||||
6256|Erskine Sandstone|22764|4|Described|Table2,p8|Middle Triassic|Early Triassic|Thickness: 50 m. Conformable on Blina Shale.||||||01-FEB-10
6256|Erskine Sandstone|22767|5|Briefly described|Table3 P14, P22|Middle Triassic|Early Triassic|||||||
6256|Erskine Sandstone|22776|4|Described|Table.3|Middle Triassic|Early Triassic|Thick: 270m.||||||13-NOV-07
6256|Erskine Sandstone|23722|6|Mentioned|p35|Triassic|Triassic|||||||
6256|Erskine Sandstone|23765|5|Briefly described|Map Legend|Triassic|Triassic|||||||
6256|Erskine Sandstone|23766|4|Described|p13 Tb. 2|Middle Triassic|Early Triassic|See also p23.  Consists of equal portions of  very fine to fine grey sandstone and grey claystone with siltstone and minor black shale.   Thickness: 265m.   Geological Province: Canning Basin.||||||17-NOV-08
6256|Erskine Sandstone|24061|5|Briefly described|p182|Triassic|Triassic|Geological Province:  Canning Basin.||||||
6256|Erskine Sandstone|24466|5|Briefly described|p368 Fig. 3|Triassic|Triassic|||||||
6256|Erskine Sandstone|29633|6|Mentioned|p435|||Upper Permian/Lower Triassic||||||
6256|Erskine Sandstone|30110|6|Mentioned|p78|||See also p83. Middle Triassic Anisian age.||||||10-FEB-20
6256|Erskine Sandstone|30287|6|Mentioned|p16|||||||||
6256|Erskine Sandstone|30547|6|Mentioned|p426|||Correlation||||||
6256|Erskine Sandstone|30565|6|Mentioned|p120|||||||||
6256|Erskine Sandstone|30897|6|Mentioned|p19|||Subsurface unit||||||
6256|Erskine Sandstone|32648|6|Mentioned|p32|||Triassic||||||
6256|Erskine Sandstone|32799|6|Mentioned|p29|||||||||
6256|Erskine Sandstone|32803|6|Mentioned|p96|||||||||
6256|Erskine Sandstone|34008|2|Defined|p68|Early Triassic|Early Triassic|||||||
6256|Erskine Sandstone|34009|6|Mentioned|Table III|||||||||
6256|Erskine Sandstone|34010|6|Mentioned|Cor. chart|||Lower - Middle Triassic.||||||13-NOV-07
6256|Erskine Sandstone|34113|6|Mentioned|p67|||Fossil vertebrate localities||||||
6256|Erskine Sandstone|34287|6|Mentioned|p151|||Triassic||||||
6256|Erskine Sandstone|35120|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early to Middle Triassic?Prob.E - M Triassic||||||
6256|Erskine Sandstone|35124|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early to Middle Triassic?Prob.E - M Triassic||||||
6256|Erskine Sandstone|35205|6|Mentioned|Map legend|Triassic|Triassic|||||||
6256|Erskine Sandstone|35275|6|Mentioned|Fig.5.|||||||||
6256|Erskine Sandstone|36224|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Very fine to fine sandstone. Early to Middle Triassic.||||||01-FEB-05
6256|Erskine Sandstone|36257|6|Mentioned|Table 2.1|||||||||
6256|Erskine Sandstone|36634|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early to Middle Triassic||||||
6256|Erskine Sandstone|36890|3|Fully described|p345|||Formerly Erskine Series.||||||13-NOV-07
6256|Erskine Sandstone|38878|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Early - Middle Triassic||||||
6256|Erskine Sandstone|40992|6|Mentioned|Fig.11|||||||||
6256|Erskine Sandstone|41169|6|Mentioned|p148|||||||||
6256|Erskine Sandstone|41215|6|Mentioned|p281|||||||||
6256|Erskine Sandstone|41449|5|Briefly described|p256|||||||||
6256|Erskine Sandstone|41688|4|Described|p13|||See also p19.||||||13-NOV-07
6256|Erskine Sandstone|41730|6|Mentioned|Fig.3|||||||||
6256|Erskine Sandstone|42734|5|Briefly described|map legend|Triassic||||||||
6256|Erskine Sandstone|42814|5|Briefly described|p24|||||||||
6256|Erskine Sandstone|42930|5|Briefly described|Fig.1 p473|Triassic|Triassic|Unconformable over Blina Shale. Geological Province: Canning Basin. Fluvial deposits.||||||13-NOV-07
6256|Erskine Sandstone|43173|6|Mentioned|12,54||Early Triassic|||||||
6256|Erskine Sandstone|43281|5|Briefly described|Map legend||Triassic|||||||
6256|Erskine Sandstone|43563|6|Mentioned|Fig.2,p5,Fig.9,p15||Scythian|||||||
6256|Erskine Sandstone|43656|6|Mentioned|Fig.2,p8|Anisian|Scythian|||||||
6256|Erskine Sandstone|43666|6|Mentioned|p45,Table 2|Anisian|Scythian|||||||
6256|Erskine Sandstone|43746|6|Mentioned|Fig.2,p11|Anisian|Scythian|||||||
6256|Erskine Sandstone|43818|6|Mentioned|Fig.2.p39|Middle Triassic|Early Triassic|||||||
6256|Erskine Sandstone|43932|4|Described|p10,Tb.1 p5|Middle Triassic|Early Triassic|||||||
6256|Erskine Sandstone|43976|6|Mentioned|p69,73|||Re geology||||||
6256|Erskine Sandstone|44143|4|Described|p.434 Table 4-19, p447-448|Triassic|Triassic|Up to 270 m thick; very fine to fine sandstone; fluvial. Disconformably overlies Blina Shale. Type section at Erskine Range (DERBY: 17deg 50' S, 124deg 22' E). Contains macroflora of equisetaleans and lycopods, microflora.||||||23-NOV-17
6256|Erskine Sandstone|44479|2|Defined|Tb.1|||E/51-1. Correlates undiff. Mesozoic of this Sheet.||||||
6256|Erskine Sandstone|44998|2|Defined|p.114-6|||Overlies Blina Shale; overlain by Meda Formation. (E51-7). On many pages. p.88,103-4,108-110,245,map. See also App.6 p294, 306 for.||||||13-NOV-07
6256|Erskine Sandstone|45153|2|Defined|App.5-89|Middle Triassic|Middle Triassic|See also App.4-72. Type section: Erskine Range (17degrees50' S, 124degrees20' E). Lithology:sandstone: grey, silty, micaceous, carbonaceous, thinly to massively bedded, fine to medi urn-grained quartzose, commonly cross-bedued, with interbeds of quartz-pebble conglomerate. Cut-and-fill structures contain clay-pellet conglomerate or conglomerate lag deposits, and ripple marks and mud-cracks sometimes occur in the interbedded siltstone. The only tossils present are trace fossils and ,plant remains.||||||15-DEC-22
6256|Erskine Sandstone|45156|6|Mentioned|p31|||Correlative||||||
6256|Erskine Sandstone|45158|3|Fully described|p16|||||||||
6256|Erskine Sandstone|45168|6|Mentioned|p6|||||||||
6256|Erskine Sandstone|46863|6|Mentioned|Fig.2|||||||||
6256|Erskine Sandstone|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
6256|Erskine Sandstone|48826|14|Not recorded|p.28|||Tb.III. Correlates with Culvida Sandstone.||||||
6256|Erskine Sandstone|48857|14|Not recorded|p.13|||||||||
6256|Erskine Sandstone|63929|6|Mentioned|p131 Fig.2.|Early Triassic|Early Triassic|Onshore Canning Basin.||||Overlies Blina Shale. Is overlain by Culvida Sandstone.||
6256|Erskine Sandstone|64187|5|Briefly described|p320 Fig. 2|Middle Triassic|Middle Triassic|Underlain by Blina Shale, overlain by alluvium material. Sandstone (continental). Geological Province: Canning Basin. +||||||15-FEB-10
6256|Erskine Sandstone|64580|4|Described|map legend|Middle Triassic|Early Triassic|Fine-grained sandstone; lesser sandy shale, minor conglomerate. Eastern Canning Basin.||||||17-NOV-08
6256|Erskine Sandstone|64643|5|Briefly described|p9, p3 Fig. 2|Middle Triassic|Early Triassic|Up to 270m of very fine to fine-grained sandstone. Type section in Erskine Range.||||||10-FEB-20
6256|Erskine Sandstone|64981|6|Mentioned|p669 Fig.3.|Anisian|Anisian|||||Overlies Blina Shale.||
6256|Erskine Sandstone|65301|5|Briefly described|p5 Fig. 4|Early Triassic|Early Triassic|Geological province: Canning Basin.||||||
6256|Erskine Sandstone|65449|6|Mentioned|p6|Middle Triassic|Early Triassic|||||Overlies Blina Shale.||
6256|Erskine Sandstone|66124|5|Briefly described|p169, p170 Fig.2|Olenekian|Olenekian|Canning Basin. Maximum 270m thick. Marine regression. Overlies Blina Shale and underlies Culvida Sandstone.||||||
6256|Erskine Sandstone|66949|4|Described|p24, p26-28, p46 Appx.2, p55 Appx.3|Ladinian|Olenekian|See also p60-65 Appx.4; p76 Appx.5. Originally Erskine Series of Wade (1937); amended to Erskine Sandstone by Guppy et al. (1952). Type section detailed. Up to 270m thick; fluvial deposits. Age from plant macrofossils, microfossils. Mud-cracks, no marine fossils. Available core and Formation picks detailed.||||Conformably overlies Blina Shale.|Massive and cross-bedded silty sandstone with interbedded conglomerate.|04-NOV-15
6256|Erskine Sandstone|68007|6|Mentioned|p4|Early Triassic|Early Triassic|Canning Basin.||||||25-FEB-20
6256|Erskine Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut|Middle Triassic|Early Triassic||||||Fine-grained sandstone; lesser sandy shale, minor conglomerate.|
6256|Erskine Sandstone|68811|6|Mentioned|p81, p127 tbl 14|Triassic|Triassic|See also p154 app 1, p174 tbl 35. ||||Overlies the Blina Shale. Overlain by the Munkayarra Shale and the Wallal Sandstone.||15-APR-20
6256|Erskine Sandstone|68902|6|Mentioned|p9 fig 5|Triassic|Triassic|||||Overlies Blina Shale.||
6256|Erskine Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Middle Triassic|Early Triassic||||||fine-grained sandstone; lesser sandy shale, minor conglomerate|
6256|Erskine Sandstone|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p15-p16|Middle Triassic|Early Triassic|Canning Basin. See also  Ch4 p30-p35, Ch4 p38, Ch4 p43-p44, Ch4 p45, Ch4 p50-p58, Ch4 p74-p77, Ch4 p84, Ch4 p88, Ch4 p90.||||Overlies the Blina Shale.||10-FEB-20
6256|Erskine Sandstone|69587|5|Briefly described|500k_geologyp08_lut.csv|Middle Triassic|Early Triassic||||||Fine-grained sandstone; lesser sandy shale, minor conglomerate|
6256|Erskine Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|Middle Triassic|Early Triassic||||||Fine-grained sandstone; lesser sandy shale, minor conglomerate|
6256|Erskine Sandstone|70154|4|Described|500k_interpgeop14_lut.csv|Middle Triassic|Lower Triassic||237-252 Ma||||Fine grained sandstone; lesser sandy shale, minor conglomerate|
6256|Erskine Sandstone|70774|5|Briefly described|p4|Early Triassic|Early Triassic|Fitzroy Trough and Lennard Shelf, Canning Basin.||||Overlies the Blina Shale.||10-FEB-20
6256|Erskine Sandstone|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Canning Basin.||||||
6256|Erskine Sandstone|70878|5|Briefly described|p722 Fig.17|Triassic|Triassic|Fitzroy Trough, NW Canning Basin.||||||
6256|Erskine Sandstone|71146|5|Briefly described|p6|Middle Triassic|Early Triassic|Canning Basin.||||Overlies the Blina Shale.|Sandstone.|
6256|Erskine Sandstone|71267|4|Described|GEOL_LUT_CSV files|Ladinian|Olenekian|Of Canning Basin. Events: Point Moody Extension (300 -242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|250-237 mA (biostrat)||||Fluvial very fine to medium grained parallel-and cross-bedded micaceous sandstone with minor siltstone and mudstone; plant macrofossils and palynomorphs|
6256|Erskine Sandstone|71894|5|Briefly described|p3-p4|Triassic|Triassic|Canning Basin. Laterally extensive across the basin.||||Overlies the Blina Shale. Unconformably overlain by the Barbwire Sandstone.|Sandstone.|
6256|Erskine Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Ladinian|Olenekian|Canning Basin.  Age from biostratigraphy.|||||Fine-grained sandstone; lesser sandy shale, minor conglomerate.|
6256|Erskine Sandstone|72497|5|Briefly described|p3 Fig.2.|Olenekian|Induan|Shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace. Age shown as later Scythian = Induan-Olenekian.||||Conformably overlies Blina Shale.||
6256|Erskine Sandstone|72499|5|Briefly described|p7 Fig.6.|Middle Triassic|Middle Triassic|Located in the Fitzroy Trough.||||Overlies Blina Shale and shown as unconformably underlying Barbwire Sandstone.||
6256|Erskine Sandstone|73117|5|Briefly described|p3, p109-110, p121|Lower Triassic|Lower Triassic|Canning Basin.||||Underlain by Blina Shale.|Dominantly sandstone.|
6256|Erskine Sandstone|73445|5|Briefly described|p3, 6, 8, 12, 24, 65-118|||Canning Basin. 40m thick.||||Overlies Blina Shale.|Massive, cross-bedded silty sandstone with localized conglomerate beds.|
6283|Estaughs Formation|23806|5|Briefly described|p1123 Fig. 2|Neoproterozoic|Neoproterozoic|Of Mount House Formation.||||||
6283|Estaughs Formation|30525|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6283|Estaughs Formation|30533|4|Described|Table 5|||Part of Mount House Group||||||
6283|Estaughs Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6283|Estaughs Formation|32660|5|Briefly described|Table 6|||||||||
6283|Estaughs Formation|32728|6|Mentioned|Fig.16|||See also Table 7||||||
6283|Estaughs Formation|36551|6|Mentioned|Table 10|||||||||
6283|Estaughs Formation|36898|6|Mentioned|p191|||||||||
6283|Estaughs Formation|37927|6|Mentioned|p512|||||||||
6283|Estaughs Formation|38157|6|Mentioned|Table X|||||||||
6283|Estaughs Formation|39210|5|Briefly described|Fig.18|||||||||
6283|Estaughs Formation|41429|6|Mentioned|p247|||||||||
6283|Estaughs Formation|42149|6|Mentioned|Table 1 P709|||||||||
6283|Estaughs Formation|42710|5|Briefly described|map legend|Proterozoic||||||||17-OCT-12
6283|Estaughs Formation|42811|5|Briefly described|p31|||of Mount House Group||||||
6283|Estaughs Formation|44140|5|Briefly described|p301 fig 4-7, p303 Tb.4-2|Neoproterozoic|Neoproterozoic|Of Mount House area. 90m thick.||Mount House Group||Conformably overlies Throssell Shale.|Purple-green siltstone and fine sandstone.|07-MAR-18
6283|Estaughs Formation|44366|14|Not recorded|p.18, Table 3||Adelaidean|Part of Mount House Group. Definition on Tech.File E/52-5.||||||
6283|Estaughs Formation|44367|14|Not recorded|map legend||Adelaidean|(Reprinted 1971). Unit of Mount House Group.||||||
6283|Estaughs Formation|48927|6|Mentioned|Table 1|||Refers Plumb (in prep.)||||||
6283|Estaughs Formation|63458|6|Mentioned|p873 Fig.2, p875, p897 Fig.19. |Ediacaran||Said to overlie Walsh Tillite transitionally p875, but all figures show this unit overlying the Throssell Shale?||Unit in Mount House Group.||||11-MAY-15
6283|Estaughs Formation|67563|6|Mentioned|p120 Fig.1|||||||||
6283|Estaughs Formation|68244|4|Described|p660-661|Neoproterozoic|Neoproterozoic|Mount House area, Kimberley region. Resistant to weathering and forms a prominent mesa (Mount Clifton) c. 250m high.||Unit of Mount House Group.||Uppermost unit of the Mount House Group. Underlain by Throssell Shale.|Muddy sandstone and siltstone.|
6283|Estaughs Formation|68473|6|Mentioned|p531, p533|||||Mount House Group||||
6283|Estaughs Formation|71267|4|Described|GEOL_LUT_CSV files|Ediacaran|Ediacaran|See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Mount House Group.|||Purple to grey fine to medium grained micaceous sandstone interbedded with green siltstone, with tabular cross-bedded blocky white orthoquartzite at the top|
6283|Estaughs Formation|71811|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Louisa Basin.||Mount House Group.|||Purple to grey, fine- to medium-grained, micaceous sandstone with interbedded green siltstone; capped by blocky, cross-bedded sandstone.|
6345|Eucla Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Middle Eocene|||||||
6345|Eucla Group|22613|6|Mentioned|p18|||||||||
6345|Eucla Group|24563|6|Mentioned|p485|Tertiary|Tertiary|||||||
6345|Eucla Group|32552|4|Described|p56-108|||Mid.-L.Miocene||||||21-JAN-16
6345|Eucla Group|32648|6|Mentioned|p32|||Tertiary||||||
6345|Eucla Group|32750|6|Mentioned|p307|||Distribution map||||||
6345|Eucla Group|33595|4|Described|Table 1|||||||||
6345|Eucla Group|34232|6|Mentioned|p75|||Miocene. Origin of cavities.||||||
6345|Eucla Group|34759|6|Mentioned|Fig.7|||Stratigraphy||||||
6345|Eucla Group|36200|6|Mentioned|p6|||||||||
6345|Eucla Group|36890|3|Fully described|p412|||||||||
6345|Eucla Group|38221|6|Mentioned|Fig.4|||Great Australian Bight Basin||||||
6345|Eucla Group|38553|6|Mentioned|p44|||||||||
6345|Eucla Group|42075|5|Briefly described|Fig.10 P250|||||||||
6345|Eucla Group|42335|5|Briefly described|p325|||||||||
6345|Eucla Group|42959|5|Briefly described|p58 Fig.3|||||||||
6345|Eucla Group|43026|5|Briefly described|Table 1,p586|||||||||
6345|Eucla Group|43040|5|Briefly described|Fig.2,p861|||||||||
6345|Eucla Group|43065|6|Mentioned|p92|||||||||
6345|Eucla Group|43814|6|Mentioned|Fig.3,p115|||||||||
6345|Eucla Group|44133|5|Briefly described|p178|Tertiary|Tertiary|Geological Province: Eucla Basin. ||||||
6345|Eucla Group|49060|5|Briefly described|Fig.15|||||||||
6345|Eucla Group|61155|5|Briefly described|p3|||Marine clastics and carbonates deposited offshore in the Great Australian Bight.||||||03-MAR-10
6345|Eucla Group|62369|5|Briefly described|p409, p410 Fig.4|Middle Miocene|Pliocene|Carbonates veneered by Roe Calcarenite. Geological Province: Eucla Basin. See also p416.||||||01-FEB-16
6345|Eucla Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
6345|Eucla Group|65942|4|Described|p74, Fig.6 p75|Early Miocene|Middle Eocene|Includes Hampton Sandstone, Wilson Bluff Limestone, Toolinna Limestone, Abrakurrie Limestone, Nullarbor Limestone, Colville Sandstone||||||28-MAY-10
6345|Eucla Group|66131|6|Mentioned|p242 Fig.2|Holocene|Eocene|||||||
6345|Eucla Group|67789|6|Mentioned|p34-35|||Eucla Basin. A suite of sedimentary rocks extending southwards below the modern continental shelf.|||Wilson Bluff, Abrakurrie, Nullarbor Limestones.|||
6345|Eucla Group|69632|5|Briefly described|p26|Cenozoic|Cenozoic|Lowry (1970).|||Includes the Abrakurrie Limestone and the Nullarbor Limestone.|Overlies Bight Basin Group.||09-OCT-18
6345|Eucla Group|69648|5|Briefly described|p4, p21, map legend|Miocene|Eocene|Eucla Basin. Marine, temperate-water, platform, carbonates dominate the basin.|||Wilson Bluff Limestone, Nullarbor Limestone||Marine platform bioclastic carbonates.|
6345|Eucla Group|70397|6|Mentioned|p1,3|||Eucla Basin.|||Includes Nullarbor Limestone, Colville Sandstone, Garford Formation, Ooldea sands, Abrakurrie Limestone, Wilson Bluff Limestone and Hampton Sandstone.|Overlain by the Nullarbor Limestone.||29-JUL-19
6345|Eucla Group|70771|5|Briefly described|p2-p3, p27|||Eucla Basin. [The author herein assigns a number of units to this group, however this is obsolete terminology].|||Includes the Wilson Bluff Limestone, Abrakurrie Limestone, Nullarbor Limestone and the Roe Calcarenite.||Calcareous sandstones and limestones.|
6345|Eucla Group|70772|6|Mentioned|p1-p2, p6-7, p22, p36, p41|Eocene|Eocene|Bight Basin.||||Unconformably overlies the Madura Formation.||
6345|Eucla Group|70802|5|Briefly described|500k_interpgeop14_lut.csv|Miocene|Miocene|Of Eucla Basin. Events: Timorese Collision (20-0.01 Ma).|23.03-5.333 Ma (inferred)||||Bioclastic limestone with basal sandstone|
6345|Eucla Group|70826|6|Mentioned|p7 tbl 4|Miocene|Oligocene|Eucla Basin.||||||
6345|Eucla Group|71270|4|Described|2_5m_interpgeop15_lut.csv|Miocene|Miocene|Of Eucla Basin. Events: Timorese Collision (20 - 0.01 Ma); Mid-Miocene transgression, 15 Ma (15 - 15 Ma).|23.03-5.333 Ma (biostrat)||||Bioclastic limestone with basal sandstone|
6345|Eucla Group|71361|5|Briefly described|ii, p15-p16, p21, p160|Cenozoic|Cenozoic|Eucla Basin. [NB This group is currently out of use and the author references older literature - Lowry 1970].|||Includes the Nullarbor Limestone, Wilson Bluff Limestone and the Abrakurrie Limestone.|||
6345|Eucla Group|71618|6|Mentioned|p124-125,127, 133|Cenozoic|Cenozoic|Geological province: Eucla Basin.|||Includes Wilsons Bluff, Abrakurrie and Nullarbor limestones.|||05-SEP-19
6345|Eucla Group|71789|6|Mentioned|p99, 100|||||||||
6345|Eucla Group|72034|5|Briefly described|500k_interpgeop16_lut|Miocene|Oligocene|Eucla Basin. Age from biostratigraphy.|||||Bioclastic limestone with sandstone near basin margin.|
6368|Eundynie Group|9766|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, siltstone, mudstone, spongolitic siltstone, calcareous sandstone, bioclastic calcarenite, bituminous siltstone, poorly indurated, lateritized cap.||||||12-JUL-13
6368|Eundynie Group|23582|5|Briefly described|Map Legend|Eocene|Eocene|Includes Hampton Sandstone.||||||27-JUN-06
6368|Eundynie Group|23584|5|Briefly described|p29|Eocene|Eocene|Overlying unit Redmine Group. Geological Province: Yilgarn Craton.||||||
6368|Eundynie Group|23817|4|Described|p429, 430|Tertiary|Tertiary|Geological Province: Bremer Basin.||||||
6368|Eundynie Group|24160|6|Mentioned|p117.|Eocene|Eocene|||||Lower part correlates with Perkolilli Shale.||
6368|Eundynie Group|24223|5|Briefly described|Map legend|Tertiary|Tertiary|Sandstone, siltstone, mudstone, spongolitic siltstone, calcareous sandstone, bioclastic calcarenite, bituminous siltstone.||||||12-JUL-13
6368|Eundynie Group|29693|6|Mentioned|p86|||||||||
6368|Eundynie Group|30144|6|Mentioned|p84|||Depositional history||||||
6368|Eundynie Group|30562|4|Described|p19|||Cainozoic age.||||||
6368|Eundynie Group|30959|6|Mentioned|Map legend|Eocene|Eocene|||||||
6368|Eundynie Group|31562|6|Mentioned|p10|||See also p12. Stratigraphic table.||||||13-SEP-18
6368|Eundynie Group|32648|6|Mentioned|p32|||Tertiary||||||
6368|Eundynie Group|32750|6|Mentioned|p306|||Refers Cockbain 1968c & Crespin in Clarke et al. (1948)||||||
6368|Eundynie Group|35059|6|Mentioned|p205|||||||||
6368|Eundynie Group|36200|6|Mentioned|p6|||||||||
6368|Eundynie Group|36890|3|Fully described|p430|||||||||
6368|Eundynie Group|40877|5|Briefly described|p55|||||||||
6368|Eundynie Group|41771|4|Described|p47|||||||||
6368|Eundynie Group|42535|6|Mentioned|p17|||||||||
6368|Eundynie Group|42724|5|Briefly described|map legend|Tertiary||||||||
6368|Eundynie Group|42817|4|Described|p27|||see also Fig.6 and Table 1||||||
6368|Eundynie Group|42959|5|Briefly described|p58 Fig.3|||||||||
6368|Eundynie Group|43065|5|Briefly described|p88|||see also Fig.5,p92||||||
6368|Eundynie Group|43498|3|Fully described|8|||||||||20-MAY-14
6368|Eundynie Group|44145|6|Mentioned|p556|Late Eocene|Late Eocene|Clastic deposition, primarily in coastal swamps. Western margin of Eucla Basin.||||||
6368|Eundynie Group|45149|6|Mentioned|p63|||||||||
6368|Eundynie Group|60076|5|Briefly described|p32, p44 App. 1|Late Eocene|Late Eocene|[Te]   Shallow water, fluviodeltaic channelled and cross-bedded sandstone, siltstone and conglomerates, increasingly interspersed with spongilite and macrofossiliferous limestone to the south.  Found in the Cowan and Lefroy palaeodrainage channels.||||||13-APR-05
6368|Eundynie Group|60555|6|Mentioned|p4 Tb. 1, p17, p18, p24|Eocene|Tertiary|Age of deposition: 50-38Ma. Marine transgression.||||||
6368|Eundynie Group|61155|5|Briefly described|p3, p17|Late Eocene|Middle Eocene|Contains the Princess Royal Spongolite and Norseman Limestone Formation. Includes bryozoal carbonates and spongolites. Age: 51.5-36.5Ma. Geological Province: Bremer Basin.||||||03-MAR-10
6368|Eundynie Group|62093|5|Briefly described|p217 Tb. 1|Eocene|Eocene|Age: 50-38Ma.||||||
6368|Eundynie Group|64340|4|Described|p4, p9, p26 Tb. 5, p26-28|Eocene|Eocene|Includes; Werrilup Formation, Norseman Formation, Pidinga Formation, North Royal Formation, Pallinup Formation, Hampton Sandstone, Princess Royal Spongolite.Sedimentary rocks. Fluviodeltaic to estuarine deposition. See p26-28 for more info.||||||12-JUL-13
6368|Eundynie Group|64622|5|Briefly described|map legends|Eocene|Eocene|Geological province:  Eucla Basin. Comprises an undivided component dominantly sandstone (further details included), and limestone which is massive to weakly bedded; locally fossiliferous with gastropod, brachiopod and bivalve fossils.||||||03-NOV-08
6368|Eundynie Group|65257|5|Briefly described|Map Legend|Eocene|Eocene|Dominant sandstone; includes conglomerate, siltstone, mudstone, spongolitic or bituminous siltstone, calcareous sandstone, and bioclastic calcarenite; generally poorly indurated, locally silicified and with common ferruginous cappings. Geol Prov: Eucla.||||||16-JUN-09
6368|Eundynie Group|65258|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, siltstone, mudstone, spongolitic siltstone, calcareous siltstone, bioclastic calcarenite, bituminous siltstone; includes poorly indurated laterized caprock.||||||16-JUN-09
6368|Eundynie Group|65260|3|Fully described|p1, p5, p6 Tb.1, p25-26|Bartonian|Ypresian|Throughout southern Eastern Goldfields Granite-Greenstone Terrane. Fluviodeltaic, estuarine to marine sediments, predominantly found within palaeodrainage channels.|50-38 Ma.||Includes Lower and Upper Werrillup and Norseman Formations, Princess Royal Spongolite, Pidinga Formation, Hampton Sandstone.||Large tabular bedded sandstone units, interbedded siltstone; mudstone, conglomerate, and iron-cemented gravel lenses, and spongolite. Silcrete and ferruginous silcrete are most commonly formed over this Group.|20-MAY-14
6368|Eundynie Group|65264|5|Briefly described|p28, p43 Appdx. 1|Late Eocene|Late Eocene|Geological province: Eucla Basin. Comprises shallow-water, fluviodeltaic channelled and crossbedded sandstone, siltstone and conglomerate.||||||07-FEB-11
6368|Eundynie Group|69152|4|Described|GEOL_LUT_CSV files + geochron files|Eocene|Eocene|Eucla Basin|||||Sandstone, conglomerate, siltstone, mudstone, spongolitic or bituminous siltstone, calcareous sandstone, and bioclastic calcarenite; generally poorly indurated, locally silicified with common ferruginous cap; fossiliferous.|05-AUG-15
6368|Eundynie Group|69598|6|Mentioned|p2, p9, p11 Tb.1, p29 Tb.4|Middle Eocene|Middle Eocene|Eucla Basin. |||Includes the Hampton Sandstone and the Norseman Formation.|Overlain by the Plantagenet Group.||
6368|Eundynie Group|70153|5|Briefly described|100k_geologyp10_lut.csv|Eocene|Eocene|Eucla Basin.|||||Sandstone, conglomerate, siltstone, mudstone, spongolitic or bituminous siltstone, calcareous sandstone, and bioclastic calcarenite. Limestone; locally fossiliferous with gastropod, brachiopod and bivalve fossils. Fossiliferous sandstone.|
6368|Eundynie Group|70802|5|Briefly described|GEOL_LUT_CSV files|Eocene|Eocene|Of Eucla Basin. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv.|||||Undivided; sandstone, conglomerate, siltstone, mudstone, spongolitic or bituminous siltstone, calcareous sandstone, and bioclastic calcarenite; generally poorly indurated, locally silicified with common ferruginous cap|
6368|Eundynie Group|70826|6|Mentioned|p7 tbl 4|Eocene|Eocene|Eucla Basin.||||||
6368|Eundynie Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, limestone|
6368|Eundynie Group|71270|4|Described|GEOL_LUT_CSV files|Eocene|Eocene|Of Eucla Basin. See 100k_geologyp10_lut.csv, 100k_geologysub10_lut.csv.|||||Undivided; sandstone, conglomerate, siltstone, mudstone, spongolitic or bituminous siltstone, calcareous sandstone, and bioclastic calcarenite; generally poorly indurated, locally silicified with common ferruginous cap|
6368|Eundynie Group|71788|14|Not recorded|p97-98, Plate 41 |||Includes Norseman Lst, Cowan Dolomite and Princes Royal Spongolite.||||||
6368|Eundynie Group|71789|6|Mentioned|p100,101|||includes Princess Royal Spongolite, Norseman Limestone.||||||
6435|Ewington Coal Measures|14227|5|Briefly described|Enclos. 2|Sakmarian|Sakmarian|Overlies Westralia Sandstone; underlies Allanson Sandstone. Presented as Ewington CM.||||||07-FEB-11
6435|Ewington Coal Measures|22820|6|Mentioned|p18|||Of the Collie Group.||||||11-AUG-08
6435|Ewington Coal Measures|23174|5|Briefly described|Fig5p8|||||||||
6435|Ewington Coal Measures|23279|6|Mentioned|p15|||(Le Blanc Smith, 1993).||||||
6435|Ewington Coal Measures|42711|2|Defined|p5 Fig. 4, p23-24, Plates 2, 4, 5|Permian|Permian|Of Collie Group. Superseded Ewington Member. Conformably over Westralia Sandstone; conformable below Allanson Sandstone. Geological province: Collie Basin. Detailed lithology given.||||||22-JUL-09
6435|Ewington Coal Measures|43442|6|Mentioned|p50|||||||||
6435|Ewington Coal Measures|62113|5|Briefly described|p626. |Permian|Permian|Collie Basin. Equivalent to Irwin River Coal Measures.||||||
6435|Ewington Coal Measures|64580|6|Mentioned|map legend|||Of Collie Group.||||||15-DEC-08
6435|Ewington Coal Measures|64630|5|Briefly described|p31 Fig.2|Kungurian|Sakmarian|Province: Collie Subbasin. Overlies the Westralia Sandstone, underlies the Allandale Sandstone. Palynology age: S. fusus to P. sinuosus. Middle correlates with Ashbrook Sandstone.||||||24-NOV-09
6435|Ewington Coal Measures|70097|5|Briefly described|p19 Fig.3|Kungurian|Sakmarian|Southern Perth Basin. Collie Sub-basin.||Collie Group|||Includes coal.|
6435|Ewington Coal Measures|70774|5|Briefly described|p5 fig 3|Kungurian|Artinskian|Collie Basin.||||Overlies the Westralia Sandstone. Overlain by the Allandale Sandstone.||
6435|Ewington Coal Measures|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Artinskian|Perth Basin.  Age from biostratigraphy.||Collie Group.|||Interbedded poorly sorted feldspathic sandstone, carbonaceus shale, coal; conglomerate.|
6446|Exmouth Sandstone|23726|5|Briefly described|p92|Quaternary|Pliocene|Overlying unit Bundera Calcarenite. Geological Province: Carnarvon Basin.||||||
6446|Exmouth Sandstone|23815|4|Described|p304, 305|Pliocene|Pliocene|Geological Province: Carnarvon Basin. Underlying units: Trealla Limestone and Pilgramunna Formation (both unconformable). Max. thickness: 12 m.||||||18-APR-05
6446|Exmouth Sandstone|24059|5|Briefly described|p139|Quaternary|Quaternary|Geological Province: Carnarvon Basin.||||||
6446|Exmouth Sandstone|24351|5|Briefly described|Plate 4 (in pocket)|Pleistocene|Pliocene|Geological Province: Exmouth Sub-basin.||||||13-DEC-07
6446|Exmouth Sandstone|30821|6|Mentioned|p59|||Stratigraphic sequence||||||
6446|Exmouth Sandstone|32648|6|Mentioned|p32|||Pleistocene||||||
6446|Exmouth Sandstone|32750|6|Mentioned|p313|||Stratigraphic table||||||
6446|Exmouth Sandstone|33593|4|Described|p113|||Divided into Muiron & Milyering Members||||||
6446|Exmouth Sandstone|35105|6|Mentioned|Fig.5|||||||||
6446|Exmouth Sandstone|35282|6|Mentioned|p27|||||||||
6446|Exmouth Sandstone|36257|6|Mentioned|Table 2.1|||||||||
6446|Exmouth Sandstone|36386|6|Mentioned|p156|||||||||
6446|Exmouth Sandstone|36890|3|Fully described|p304|||Includes Vlaming Sandstone||||||
6446|Exmouth Sandstone|37016|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
6446|Exmouth Sandstone|39427|4|Described|Table 1|||||||||
6446|Exmouth Sandstone|40617|6|Mentioned|p18|||||||||
6446|Exmouth Sandstone|41271|3|Fully described|p194|||||||||
6446|Exmouth Sandstone|41438|6|Mentioned|Fig.23|||||||||
6446|Exmouth Sandstone|41444|6|Mentioned|Fig.4|||||||||
6446|Exmouth Sandstone|42116|5|Briefly described|p71|||||||||
6446|Exmouth Sandstone|44657|14|Not recorded|p.5|||||||||
6446|Exmouth Sandstone|44959|3|Fully described|p.30|||||||||
6446|Exmouth Sandstone|46805|6|Mentioned|Fig.2|||||||||
6446|Exmouth Sandstone|46983|6|Mentioned|Fig.2|||||||||
6446|Exmouth Sandstone|61155|5|Briefly described|p15|Holocene|Late Pliocene|Partly overlies Nadarra Sandstone; overlain by Bundera Calcarenite.  Age: <2Ma.  Geological Province: Carnarvon Basin /onshore.||||||03-MAR-10
6446|Exmouth Sandstone|62837|5|Briefly described|Stratigraphic columns|Quaternary|Quaternary|Age: >0.0Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
6446|Exmouth Sandstone|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore. Occupies a terrace between Jurabi and Muiron Scarps.|||Milyering, Muiron Members.|Overlies Pilgramunna Formation.|Coarse-grained littoral deposits overlain by medium-grained aeolian deposits.|
6446|Exmouth Sandstone|67200|5|Briefly described|p8 fig 6,p17 table 1 |Quaternary|Pliocene|Thermal conductivity of 1.42 W/mK||||Overlies Pilgramunna Formation, Vlaming Sandstone, overlain by Bundera Calcarenite|Planar cross bedded sandstone and limestone with invertebrate macrofossils.|
6446|Exmouth Sandstone|69182|6|Mentioned|Ch3 p71|||||||Overlies the Trealla Limestone.||
6446|Exmouth Sandstone|69558|6|Mentioned|p99|||||||May be equivalent to the Tamala Limestone.||
6446|Exmouth Sandstone|70066|5|Briefly described|Regional: Fig.6|Holocene|Pleistocene|Exmouth Sub-basin, Northern Carnarvon Basin.||||Overlies Pilgramunna Formation.||
6446|Exmouth Sandstone|70826|6|Mentioned|p7 tbl 4|Quaternary|Quaternary|Northern Carnarvon Basin.||||||
6446|Exmouth Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite, conglomerate, sandstone|
6467|Fair Adelaide Syenogranite|41786|6|Mentioned|Fig.2|||Reserved as Fair Adelaide Granite||||||
6467|Fair Adelaide Syenogranite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
6467|Fair Adelaide Syenogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6467|Fair Adelaide Syenogranite|60076|5|Briefly described|p46 App. 1|||[Agyad]   Medium-grained, equigranular and massive.||||||
6467|Fair Adelaide Syenogranite|65204|6|Mentioned|p19 Tbl.4,|Neoarchean||3-4mm grains; equigranular||||||
6467|Fair Adelaide Syenogranite|65264|5|Briefly described|p46 Appdx. 1|Archean|Archean|Medium grained, equigranular, massive syenogranite.||||||07-FEB-11
6467|Fair Adelaide Syenogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained, equigranular, massive syenogranite; contacts discordant with greenstones and early foliation in granitic rock.|05-AUG-15
6467|Fair Adelaide Syenogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Medium-grained, equigranular, massive syenogranite; contacts discordant with greenstones and early foliation in granitic rock.|
6467|Fair Adelaide Syenogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenogranite|
6467|Fair Adelaide Syenogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|3010-2600 Ma (inferred)||||Medium-grained, equigranular, massive syenogranite; contacts discordant with greenstones and early foliation in granitic rock|
6483|Fairfield Group|7433|6|Mentioned|p25 Fig.2, p29. |Early Carboniferous|Late Devonian|Canning Basin; Lennard Shelf, Jurgurra and Barbwire Terraces. Shallow marine clastics and carbonates.||||||
6483|Fairfield Group|14228|5|Briefly described|p6 fig3|Carboniferous|Devonian|North Canning Basin.||||Overlain by Anderson Formation.||05-OCT-16
6483|Fairfield Group|22741|5|Briefly described|P23, Table3 P15||Devonian|||||||
6483|Fairfield Group|22753|5|Briefly described|Fig.3 p585|Carboniferous|Devonian|||||||
6483|Fairfield Group|22764|6|Mentioned|p13|||May correlate with Undivided Middle Devonian to Early Carboniferous rocks||||||01-FEB-10
6483|Fairfield Group|22765|6|Mentioned|P9|Early Carboniferous|Early Devonian|||||||
6483|Fairfield Group|22767|6|Mentioned|P20|||Supersedes the Fairfield Formation||||||
6483|Fairfield Group|22776|6|Mentioned|Table.3|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|22814|5|Briefly described|fig2|Carboniferous|Carboniferous|||||||
6483|Fairfield Group|23338|5|Briefly described|915 Fig.3|Late Devonian|Late Devonian|||||||
6483|Fairfield Group|23522|5|Briefly described|p245|Tournaisian|Famennian|||||||
6483|Fairfield Group|23523|5|Briefly described|p994 Fig. 2|Carboniferous|Carboniferous|||||||
6483|Fairfield Group|23722|4|Described|p34|Early Carboniferous|Late Devonian|Max. thickness: 116m.   Geological Province: Canning Basin||||||
6483|Fairfield Group|23765|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||23-DEC-09
6483|Fairfield Group|23766|4|Described|p14 Tb. 2|Early Carboniferous|Late Devonian|See also p15.||||||
6483|Fairfield Group|23847|5|Briefly described|p297 Fig. 1|Early Carboniferous|Late Devonian|Geological Province: Canning Basin.||||||
6483|Fairfield Group|23903|5|Briefly described|p1596, p1597 Fig. 2|Tournaisian|Famennian|Geological Province: Canning Basin.||||||10-NOV-08
6483|Fairfield Group|24390|5|Briefly described|p6 Fig. 4|Carboniferous|Devonian|Geological Province: Canning Basin.||||||
6483|Fairfield Group|36115|6|Mentioned|Fig.1|||||||||
6483|Fairfield Group|36224|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Includes: Laurel Formation, Yellow Drum Sandstone and the Gumhole Formation. Late Devonian to Early Carboniferous.||||||01-FEB-05
6483|Fairfield Group|36225|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous||||||
6483|Fairfield Group|36257|6|Mentioned|Table 2.1|||||||||
6483|Fairfield Group|36365|6|Mentioned|p815|||||||||
6483|Fairfield Group|36634|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
6483|Fairfield Group|38207|6|Mentioned|Fig.1|||||||||
6483|Fairfield Group|38277|6|Mentioned|p154|||||||||
6483|Fairfield Group|38878|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
6483|Fairfield Group|39702|6|Mentioned|Fig.2|||||||||
6483|Fairfield Group|40793|6|Mentioned|Fig.3|||||||||
6483|Fairfield Group|40838|6|Mentioned|p278|||See also P279||||||
6483|Fairfield Group|40866|6|Mentioned|p181|||||||||
6483|Fairfield Group|40992|6|Mentioned|p17|||Mention Fig.11||||||
6483|Fairfield Group|41023|4|Described|p287|||||||||
6483|Fairfield Group|41139|6|Mentioned|Fig.2|||||||||
6483|Fairfield Group|41158|6|Mentioned|p73|||||||||
6483|Fairfield Group|41169|6|Mentioned|p147|||||||||
6483|Fairfield Group|41217|6|Mentioned|p310|||||||||
6483|Fairfield Group|41283|6|Mentioned|p77|||||||||
6483|Fairfield Group|41436|6|Mentioned|p39|||||||||
6483|Fairfield Group|41492|5|Briefly described|p114|||||||||
6483|Fairfield Group|41593|6|Mentioned|p15|||||||||
6483|Fairfield Group|41688|5|Briefly described|Table 4|||||||||
6483|Fairfield Group|41730|6|Mentioned|p470|||||||||
6483|Fairfield Group|41828|6|Mentioned|Table 1|||||||||
6483|Fairfield Group|41839|4|Described|p21|||Formerly "Fairfield Formation"||||||
6483|Fairfield Group|41894|5|Briefly described|p4|||||||||
6483|Fairfield Group|42030|5|Briefly described|Fig.2 P744|||||||||
6483|Fairfield Group|42191|6|Mentioned|p437|||||||||
6483|Fairfield Group|42347|5|Briefly described|p1019, Fig.2 p1020|Early Carboniferous|Late Devonian|See also Fig.12 p 1033||||||
6483|Fairfield Group|42351|5|Briefly described|p38|Tournaisian|Famennian|See also Fig.3 P40. Age latest Famennian to earliest Tournaisian.||||||
6483|Fairfield Group|42547|4|Described|p92|||||||||
6483|Fairfield Group|42564|5|Briefly described|p10|||||||||
6483|Fairfield Group|42583|5|Briefly described|p65|||||||||
6483|Fairfield Group|42710|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|42811|3|Fully described|p43|||||||||
6483|Fairfield Group|42814|4|Described|p23|||probable Late Devonian age||||||
6483|Fairfield Group|42815|5|Briefly described|map|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|42860|5|Briefly described|Fig.2|||||||||
6483|Fairfield Group|42880|5|Briefly described|p1020|||||||||
6483|Fairfield Group|42994|6|Mentioned|p13|||||||||
6483|Fairfield Group|43142|5|Briefly described|p188|||||||||
6483|Fairfield Group|43173|6|Mentioned|54||Early Carboniferous|||||||
6483|Fairfield Group|43281|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|43563|6|Mentioned|Fig.2,p6,Fig.5,p10|Tournaisian|Famennian|||||||
6483|Fairfield Group|43656|6|Mentioned|Fig.2,p8|Tournaisian|Famennian|||||||
6483|Fairfield Group|43666|6|Mentioned|p24|||||||||
6483|Fairfield Group|43723|6|Mentioned|p62|||||||||
6483|Fairfield Group|43746|6|Mentioned|Fig.2,p11|Tournaisian|Famennian|||||||
6483|Fairfield Group|43815|6|Mentioned|Table 1,p95-96|||||||||
6483|Fairfield Group|43818|6|Mentioned|Fig.2.p39|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|43819|6|Mentioned|Fig.2,p34|||||||||
6483|Fairfield Group|44143|6|Mentioned|p442, p437 Tb. 4-19, p.443|Early Carboniferous|Late Devonian|Includes Laurel and Gumhole Formations and Yellow Drum Sandstone. Shallow marine carbonates and siliciclastics. Richly fossiliferous in parts.||||||23-NOV-17
6483|Fairfield Group|44231|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Limestone, sandstone, siltstone, and shale; shallow marine deposits.  Geological Province: Canning Basin.||||||18-MAY-05
6483|Fairfield Group|45133|4|Described|p2|||||||||
6483|Fairfield Group|45143|2|Defined|p7|Tournaisian|Famennian|Famenian to Tournasian||||||
6483|Fairfield Group|45153|4|Described|App.3-33|||||||||
6483|Fairfield Group|45158|3|Fully described|p22|||See also pp 22 & 41||||||22-JAN-13
6483|Fairfield Group|46794|5|Briefly described|p63|||||||||
6483|Fairfield Group|46869|6|Mentioned|Fig.1|||||||||
6483|Fairfield Group|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
6483|Fairfield Group|47040|6|Mentioned|p150|||||||||
6483|Fairfield Group|48978|3|Fully described|p2|Early Carboniferous|Late Devonian|See also p4 etc. U.Dev-L.Carb. Geochemistry||||||22-JAN-13
6483|Fairfield Group|50085|5|Briefly described|p6 Fig. 4|Early Carboniferous|Late Devonian|Geological Province: Canning Basin.||||||
6483|Fairfield Group|60899|5|Briefly described|p913 Fig. 2|Devonian|Devonian|In the northern Chedda Cliffs area. Geological Province: Canning Basin.||||||11-APR-06
6483|Fairfield Group|61021|5|Briefly described|p36 Fig. 2|Visean|Tournaisian|Geological Province: Canning Basin.||||||17-DEC-07
6483|Fairfield Group|61023|5|Briefly described|p10 Fig. 6|Carboniferous|Devonian|Geological Province: Canning Basin.||||||10-APR-08
6483|Fairfield Group|61139|5|Briefly described|p42 Fig. 4|Early Carboniferous|Devonian|Geological Province: Canning Basin.||||||
6483|Fairfield Group|61551|6|Mentioned|p351 Fig.2, p359, p361.|Tournaisian|Famenian|Includes oil and gas producing units in the Blina oil field.|||Includes Nullara and Yellow Drum Formations.|||
6483|Fairfield Group|62837|5|Briefly described|Stratigraphic columns|Early Carboniferous|Early Carboniferous|Age: 355-347. Geological Province:  Fitzroy Trough.||||||01-MAR-10
6483|Fairfield Group|63605|5|Briefly described|p1002|Famennian|Famennian|Geological Province: Canning Basin in W.A. Has a few acritarchs in common with the Worange Point Formation, high in the unit.||||||07-FEB-11
6483|Fairfield Group|63938|5|Briefly described|p50 Fig.2|Tournasian|Famennian|||||||
6483|Fairfield Group|64187|5|Briefly described|p320 Fig. 2|Early Carboniferous|Famennian|Underlain by Lennard River Group. Geological Province: Canning Basin.||||||15-FEB-10
6483|Fairfield Group|64502|5|Briefly described|p764, p765 Fig. 2|Tournaisian|Famennian|||||||
6483|Fairfield Group|64580|4|Described|map legend|Tournaisian|Famennian|Limestone, shale, siltstone, sandstone; includes GUMHOLE FORMATION, YELLOW DRUM SANDSTONE, and LAUREL FORMATION.||||||09-DEC-08
6483|Fairfield Group|64643|5|Briefly described|p3 Fig. 2, p18, 35|Missippippian|Missippippian|||||||
6483|Fairfield Group|64694|6|Mentioned|p248|||Canning Basin.||||||
6483|Fairfield Group|64971|5|Briefly described|p685 Fig. 2, p691 Fig. 9|Carboniferous|Visean|Overlian by Anderson Formation.||||||09-FEB-10
6483|Fairfield Group|64981|5|Briefly described|p667, p670.|Early Carboniferous|Famennian||||Includes Laurel, Yellow Drum and Gumhole Formations.|Is overlain by Anderson Formation.||
6483|Fairfield Group|65214|6|Mentioned|p280|Devonian|Devonian|Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
6483|Fairfield Group|65301|5|Briefly described|p5 Fig. 4, p8 Fig. 5|Mississippian|Mississippian|Contains the Gumhole, Yellow Drum and Laurel Formations. Geological province: Canning Basin.||||||01-FEB-10
6483|Fairfield Group|65449|5|Briefly described|p5-6|Early Carboniferous|Early Carboniferous|Fitzroy Trough and Gregory Sub-basin, Canning Basin. Mixed siliciclastic-carbonate rocks.|||Gumhole, Yellow Drum and Laurel Formations.|Is overlain by Anderson Formation.||
6483|Fairfield Group|65486|5|Briefly described|p2-4,6,9,13,18,57; Figs.2,5,7; Plate 1.|Tournaisian|Late Famennian|Post-reef shale, sandstone and siltstone in the Canning Basin. Unconformably overlies Piker Hills Formation, Windjana Limestone, and Nullara Limestone. Underlies Carolyn Formation (Grant Group). Tilted, faulted and mildly folded in Early and Middle Carboniferous.||||||
6483|Fairfield Group|66127|3|Fully described|p8, pp19-21, p81, p209, Pl 2, 3, 4, 5, 7|Tournaisian|Late Famennian|Deposited during a transgression following late Famennian sea level fall that ended formation of Canning Basin reef complexes. No outcrop in Plate 6 area; shown in Map section only.|||Includes Gumhole and Laurel Formations and Yellow Drum Sandstone.|Overlies Piker Hills Formation and Bugle Gap Limestone; unconformably overlies Windjana and Nullara Limestones. Is overlain locally by Grant Group.|Shale, sandstone and fossiliferous limestone.|
6483|Fairfield Group|66949|6|Mentioned|p28, p51 Appx.2; p79,87 Appx.5|Early Carboniferous|Early Carboniferous|Petroleum is produced from the base of this unit in the Blina field. Available core detailed.||||||
6483|Fairfield Group|67131|6|Mentioned|p2-5, 9-10|Tournaisian|Famennian|Much of this unit's lithostratigraphy is diachronous. Controversy over sequence boundary and suggestions that Group members may be part of the late Fammenian reef complex as opposed to ramp complex. Retispora lepidophyta commonly found within and used as an indicator of the base of the Fairfield Group (May River Shale).||Ramp Complex|Includes May River Shale, Gumhole Formation, Yellow Drum Formation, Laurel Formation.||A mixed siliciclastic and carbonate ramp complex.|
6483|Fairfield Group|67888|6|Mentioned|p43|Carboniferous|Devonian|||||||
6483|Fairfield Group|68007|6|Mentioned|p4|Carboniferous|Carboniferous|Canning Basin.||||||18-MAR-20
6483|Fairfield Group|68297|5|Briefly described|p186, 197|Tournasian|Famennian|WA. Includes Late Devonian vertebrate fossil assemblages, including sharks.||||||22-JAN-13
6483|Fairfield Group|68902|5|Briefly described|p9 fig 5|Carboniferous|Carboniferous|Overlies (mainly Upper) Devonian reef complexes.|||Includes Laurel, Yellow Drum, Gumhole Formations.|Is overlain by Anderson Formation.||
6483|Fairfield Group|69029|5|Briefly described|p319,322|Famennian|Famennian|Of Canning Basin. Reservoirs in the Fairfield Group are sealed by interbedded basinal shales and tight limestones in the Laurel Formation and equivalents.||||Overlain by Anderson Formation.||
6483|Fairfield Group|69099|4|Described|500k_geologyp08_lut.csv|Tournasian|Famennian||||Includes Gumhole Formation, Yellow Drum Sandstone, Laurel Formation||Limestone, shale, siltstone, sandstone.|31-JUL-15
6483|Fairfield Group|69165|4|Described|500k_geologyp08_lut.csv|Tournaisian|Famennian||||||Undivided; limestone, shale, siltstone and sandstone|
6483|Fairfield Group|69182|6|Mentioned|Ch4 p3, Ch4 p9, Ch4 p13-p14|Tournaisian|Famennian|Canning Basin. May be up to 3000m thick. See also  Ch4 p36, Ch4 p39, Ch4 p42, Ch4 p45, Ch4 p50-p58, Ch4 p63-p64, Ch4 p74-p78, Ch4 p84, Ch4 p86, Ch4 p88, Ch4 p90. |||Includes the Gumhole Formation, Yellow Drum Formation, the Yulleroo Formation and the Laurel Formation.||Shallow marine carbonates, sands and claystones.|
6483|Fairfield Group|69206|6|Mentioned|p2|Carboniferous|Carboniferous|Canning Basin.||||||
6483|Fairfield Group|69297|6|Mentioned|p337, p351, p352|Tournaisian|Famennian|Broome Platform of the Canning Basin. |||Includes the Gumhole Formation, Yellow Drum Sandstone and the Laurel Formation.|Unconformably overlain by the Reeves Formation and the Grant Group.||
6483|Fairfield Group|69312|6|Mentioned|p3, p30|Tournaisian|Famennian|Canning Basin. |||Includes the Gumhole, Yellow Drum and Laurel Formations.|Overlies the Nullara Sequence. Overlain by the Anderson Formation.||
6483|Fairfield Group|69634|5|Briefly described|500k_geologyp08_lut.csv|Tournaisian|Famennian||||Includes Gumhole Formation, Yellow Drum Sandstone and Laurel Formation.||Undivided; limestone, shale, siltstone, sandstone|
6483|Fairfield Group|69693|6|Mentioned|p3|Carboniferous|||||Laurel Formation.|Is overlain by Anderson Formation.||
6483|Fairfield Group|70065|5|Briefly described|Rowley: Fig.2. Regional: Fig.4; p6|Tournaisian|Tournaisian|Roebuck Basin and offshore Canning Basin.|||Laurel Formation.|Overlies Pillara Limestone (Reef Complex). Is overlain by Grant Group.||
6483|Fairfield Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Tournaisian|Famennian|See also 500k_interpgeop14_lut.csv.|347-372 Ma||||Limestone, Shale, Siltstone and sandstone.|
6483|Fairfield Group|70272|5|Briefly described|p878|Late Devonian|Late Devonian|Lennard shelf, Canning Basin. Up to 530m thick.|||Gumhole Formation.|Overlies Pillara Limestone. Is overlain unconformably by the Grant Group.|Shallow-marine carbonates and clastics.|
6483|Fairfield Group|70288|6|Mentioned|p415, 417|||Ellendale Diamond Mine area, 130 km ESE of Derby.|||||Includes carboniferous siltstones; intruded by an olivine lamproite dyke.|
6483|Fairfield Group|70492|5|Briefly described|p164-167, 174-176, 178-181|Early Carboniferous|Late Devonian|Lennard Shelf, northern margin of the Canning Basin. A major mixed carbonate-siliciclastic ramp system; exposed in only a few low-lying outcrops. Comprises thirteen facies associations, each described in detail: well core logs, photographs. Sequence stratigraphy, biostratigraphy detailed.|~350 Ma minimum.||Gumhole, Yellow Drum, Laurel Formations; May River Shale.|Overlies Napier Formation. Is overlain by Anderson Formation or, unconformably, by the Grant Group.||
6483|Fairfield Group|70774|5|Briefly described|p4|Mississippian|Late Devonian|Fitzroy Trough and Lennard Shelf, Canning Basin.|||Includes the Gumhole Formation, Yellow Drum Formation and the Laurel Formation.|||10-FEB-20
6483|Fairfield Group|70826|6|Mentioned|p6 tbl 3|Early Carboniferous|Late Devonian|||||||
6483|Fairfield Group|71146|5|Briefly described|p6,  p43 fig 33, p43|Tournaisian|Famennian|Canning Basin.||||Unconformably overlain by the Anderson Formation.|Sandstone, conglomerate, carbonate and mudstone.|
6483|Fairfield Group|71267|4|Described|GEOL_LUT_CSV files|Tournaisian|Famennian|Of Fitzroy Trough, Lennard Shelf, Canning Basin. Events: Fitzroy Movement (237-199 Ma); Point Moody Extension (300-242 Ma); Meda Transpression (323-310 Ma); Red Bluffs Extension (372.2-360 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Pillara Movement (Alice Springs Orogeny). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|362-346.7 Ma (biostrat)||Includes Gumhole Formation, Laurel Formation, Yellow Drum Formation.||Limestone, shale, siltstone, sandstone, dolomite; shallow marine deposits.|
6483|Fairfield Group|71870|6|Mentioned|p3|Tournaisian|Famennian|Canning Basin.||||Overlain by the Anderson Formation.||
6483|Fairfield Group|71892|6|Mentioned|p4, p10, p30 Fig.45|Paleozoic|Paleozoic||||||Includes siltstone.|
6483|Fairfield Group|71894|5|Briefly described|p3-p4|Devonian|Devonian|Canning Basin; only present in  the north of the basin based on well intersections.|||Includes the Yellow Drum Formation and the Laurel Formation.|||
6483|Fairfield Group|72034|5|Briefly described|500k_interpgeop16_lut|Tournaisian|Famennian|Fitzroy Trough; Lennard Shelf, Canning Basin.  Age from biostratigraphy.|||||Limestone, shale, siltstone, sandstone.|
6483|Fairfield Group|72496|5|Briefly described|p220, 224, 227, p229|Tournaisian|Tournaisian|Canning Basin. Deposited in a shallow marine environment.||||Overlain by the Anderson Formation and the Grant Group.|Limestone and mudstone.|18-MAR-20
6483|Fairfield Group|72497|5|Briefly described|p3 Fig.2.|Tournaisian|Famennian|Shown as occuring in the Jurgurra and Barbwire Terraces and Broome Platform. Also shown as occuring in the Fitzroy Trough, Betty and Balgo Terraces and part of the Lennard Shelf and Margaret Terrace.||||Conformably overlies Babrongian Reef Complex, Clanmeyer Formation and Luluigui Formation. Apparently conformably to unconformably overlain by Anderson Formation.||
6483|Fairfield Group|72499|4|Described|p7 Fig.6, p90 App.3.4.|Tournaisian|Fammennian|Located in the Fitzroy Trough.|||Laurel Formation, Yellow Drum Formation, ?Gumhole Formation.|Underlies Anderson Formation, Grant Group. Shown as unconformably overlying Pillara Formation.||
6483|Fairfield Group|72502|5|Briefly described|p2-5|Tournaisian|Famennian|Canning Basin.|||Gumhole Formation, Yellow Drum Formation, Laurel Formation||Includes carbonate, mudstone and sandstone.|
6483|Fairfield Group|73117|6|Mentioned|p3, p19, p70, p109, p124, p142|Tournaisian|Tournaisian|Canning Basin. Lies within the G. frustulentus Microflora.|||Laurel Formation, Yellow Drum Formation, Gumhole Formation.|Unconformably overlain by Reeves Formation and Grant Group. Unconformably? overlain by Anderson Formation.||
6577|Fenelon Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228 Fig. 18|Late Cretaceous|Late Creatceous|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
6577|Fenelon Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||||
6577|Fenelon Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||||
6577|Fenelon Formation|13354|6|Mentioned|p375 Fig.6.|Late Cretaceous|Late Cretaceous|Unit of Bathurst Island Group. Overlies Woolaston Formation and underlies Puffin Formation.||91||||28-OCT-14
6577|Fenelon Formation|22663|5|Briefly described|AC97 1-4 Fig.4|Late Cretaceous|Cretaceous|Of the Bathurst Island Group.||||||01-MAR-10
6577|Fenelon Formation|23378|5|Briefly described|p180 Fig.2||Cretaceous|Of Bathurst Island Group, Vulcan Sub-basin.||||||01-MAR-10
6577|Fenelon Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
6577|Fenelon Formation|24207|5|Briefly described|p218, p209 Fig. 5|Early Cretaceous|Early Cretaceous|Geological Province: Vulcan Sub-basin.||||||01-MAR-10
6577|Fenelon Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
6577|Fenelon Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
6577|Fenelon Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
6577|Fenelon Formation|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
6577|Fenelon Formation|60385|6|Mentioned|p270, p272 Fig 3, p276, 277, 280|Campanian|Cenomanian|Browse Basin. |||||Pelagic marl, hemipelagic marl.|
6577|Fenelon Formation|60634|6|Mentioned|p1168 Fig.3. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Gibson Formation. Is overlain by Puffin and Borde Formations.||
6577|Fenelon Formation|60709|5|Briefly described|p831 Fig. 4|Campanian|Campanian|Calcareous claystone. Geological Province: Vulcan Sub-basin.||||||
6577|Fenelon Formation|61548|6|Mentioned|p480 Fig.3|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||||
6577|Fenelon Formation|61550|6|Mentioned|p495 Fig.2. |Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Gibson Formation. Is overlain by Puffin Formation.||
6577|Fenelon Formation|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Age: ~82-~77Ma. Geological Province: Vulcan Sub-basin, Londonderry High and Northern Bonaparte Basin.||||||01-MAR-10
6577|Fenelon Formation|63358|5|Briefly described|p4 Fig. 1.3|Campanian|Santonian|See also p133 Fig. 3.71.||||||01-MAR-10
6577|Fenelon Formation|64693|5|Briefly described|p375, p377|Campanian|Campanian|Upward-fining.||||Is overlain by Puffin Sandstone.||
6577|Fenelon Formation|64695|5|Briefly described|p262 Fig.8 |Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Overlies Gibson Formation. Is overlain by Turnstone Formation.||
6577|Fenelon Formation|64697|5|Briefly described|p84 Fig.2|Late Cretaceous|Late Cretaceous|||||||
6577|Fenelon Formation|66187|5|Briefly described|p413 Fig.2|Late Cretaceous|Late Cretaceous|Bathurst Island Group. Underlies the Puffin Formation, overlies the Gibson Formation. Mount Ashmore Dome.||||||
6577|Fenelon Formation|68223|6|Mentioned|p178 Fig.3|Campanian|Campanian|||||||
6577|Fenelon Formation|69297|6|Mentioned|p305|Campanian|Santonian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Bathurst Island Group||Overlies the Gibson Formation. Overlain by the Puffin Formation.||
6577|Fenelon Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
6577|Fenelon Formation|70061|5|Briefly described|Regional geology; Figs.6-7. Sahul: Fig.2|Campanian|Campanian|See also Vulcan: Fig.2.||Bathurst Island Group.||Overlies Brown Gannet Limestone. Is overlain by Turnstone Formation.||12-JUL-16
6577|Fenelon Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2; p2|Campanian|Campanian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin. Not present in Yampi and Leveque Shelves. Potential reservoir.||Bathurst Island Group.||Overlies Brown Gannet Limestone. Is overlain by Puffin Formation.||12-JUL-16
6664|Finlay Range Gabbro|30389|6|Mentioned|p13|||||||||
6681|Fish Hole Dolerite|22754|5|Briefly described|p7|||||||||
6681|Fish Hole Dolerite|30759|6|Mentioned|p16|||Map of East Kimberley Region||||||
6681|Fish Hole Dolerite|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
6681|Fish Hole Dolerite|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6681|Fish Hole Dolerite|32660|5|Briefly described|Table 3|||||||||
6681|Fish Hole Dolerite|32728|6|Mentioned|Fig.3|||||||||
6681|Fish Hole Dolerite|33443|6|Mentioned|p260|||||||||
6681|Fish Hole Dolerite|36551|6|Mentioned|p27|||||||||
6681|Fish Hole Dolerite|36885|5|Briefly described|p176|||||||||
6681|Fish Hole Dolerite|37462|4|Described|Table4.III|||||||||
6681|Fish Hole Dolerite|44140|5|Briefly described|p293, p294 Tb.4-1, p296-297, p299|Paleoproterozoic|Paleoproterozoic|Up to 900 m thick.||||Sills intrude Red Rock beds. Probably correlative of the Hart Dolerite.|Epidotized amygdaloidal dolerite.|07-MAR-18
6681|Fish Hole Dolerite|44155|6|Mentioned|p251, p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|||||Intrudes Red Rock Beds.||
6681|Fish Hole Dolerite|44317|4|Described|Table 2||Carpentarian|||||||
6681|Fish Hole Dolerite|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
6681|Fish Hole Dolerite|45047|5|Briefly described|p28|||Carpentarian||||||
6681|Fish Hole Dolerite|60724|5|Briefly described|p18, p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|Dominated by epidotised amygdaloidal basalt interbedded with thin beds of fine sandstone and carbonate. ||||||07-NOV-08
6681|Fish Hole Dolerite|65413|6|Mentioned|p105 Fig.1, p106 Fig.2.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
6681|Fish Hole Dolerite|72437|6|Mentioned|p14|||Name presented on existing maps that the author refers to as the Red Rock Beds.||||||
6692|Fishery Hill Lamproite|41158|6|Mentioned|Table 46|||||||||
6696|Fitzgerald Peaks Syenite|22635|6|Mentioned|p483||Proterozoic|||||||
6696|Fitzgerald Peaks Syenite|24165|5|Briefly described|Plate 1|Paleoproterozoic|Paleoproterozoic||||||Syenite and quartz syenite.|
6696|Fitzgerald Peaks Syenite|35707|6|Mentioned|p153|||||||||
6696|Fitzgerald Peaks Syenite|37460|5|Briefly described|p188|||See also Fig.3.21||||||
6696|Fitzgerald Peaks Syenite|39163|3|Fully described|p56|||Age, petrograghy see P58-59.||||||09-DEC-08
6696|Fitzgerald Peaks Syenite|42793|6|Mentioned|Fig.1 P230|||||||||
6696|Fitzgerald Peaks Syenite|43203|5|Briefly described|Map Legend||Proterozoic|||||||
6696|Fitzgerald Peaks Syenite|43498|5|Briefly described|1,4||Proterozoic|Whole Rock Isochron Age: 2350Ma.||||||09-DEC-08
6696|Fitzgerald Peaks Syenite|64580|4|Described|map legend||Paleoproterozoic|Syenite and quartz syenite.||||||09-DEC-08
6696|Fitzgerald Peaks Syenite|69152|5|Briefly described|500k_geologyp08_lut||Paleoproterozoic||||||Syenite and quartz syenite.|05-AUG-15
6696|Fitzgerald Peaks Syenite|69559|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic||||||Syenite and quartz syenite.|
6696|Fitzgerald Peaks Syenite|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean||2655 +/- 3 Ma (isotopic).||||Syenite and quartz syenite.|
6696|Fitzgerald Peaks Syenite|70156|4|Described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma).|2655+\-3 Ma (isotopic)||||Syenite and quartz syenite|
6696|Fitzgerald Peaks Syenite|70794|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Neoarchean|Yilgarn Craton. Also 2_5m_interpgeop15_lut.csv.|2655+/-3 Ma||||Syenite and quartz syenite.|
6696|Fitzgerald Peaks Syenite|70802|5|Briefly described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma). See 500k_interpgeop14_lut.csv, 250k_pre_mesozoic_interpgeop_lut.csv.|2655+\-3 Ma||||Syenite and quartz syenite|
6696|Fitzgerald Peaks Syenite|70826|6|Mentioned|p9|Neoarchean|Neoarchean|||||||
6696|Fitzgerald Peaks Syenite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2655+\-3 Ma||||Syenite and quartz syenite|
6696|Fitzgerald Peaks Syenite|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||2655+/-3 Ma.||||Syenite and quartz syenite.|
6698|Fitzmaurice Group|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, shale, conglomerate.||||||
6698|Fitzmaurice Group|9538|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone. shale, siltstone, dolomite, conglomerate.  Age: <900Ma.||||||28-OCT-04
6698|Fitzmaurice Group|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.|||Includes Moyle River Formation.|Shown as unconformably overlain by the Daly River Group.||10-NOV-14
6698|Fitzmaurice Group|14019|5|Briefly described|p2 Fig. 1, p3 Fig. 2|||Succession of unmetamorphosed, but strongly folded and faulted clastic sediments.||||||
6698|Fitzmaurice Group|22809|6|Mentioned|map|Proterozoic|Proterozoic|||||||
6698|Fitzmaurice Group|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, shale, conglomerate.||||||19-OCT-05
6698|Fitzmaurice Group|24122|6|Mentioned|p2 Fig.1|||||||||
6698|Fitzmaurice Group|24297|6|Mentioned|p2 Fig.1|||||||||
6698|Fitzmaurice Group|32307|4|Described|Table 2|||Proterozoic||||||
6698|Fitzmaurice Group|32309|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian/Adelaidean||||||
6698|Fitzmaurice Group|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
6698|Fitzmaurice Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6698|Fitzmaurice Group|32660|4|Described|Table 6|||||||||
6698|Fitzmaurice Group|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Moyle River, Goodaieri and Legune Formations and the Lalngang Sandstone.||||||02-DEC-04
6698|Fitzmaurice Group|32701|4|Described|Table 1|||Adelaidean. See p7.||||||18-SEP-06
6698|Fitzmaurice Group|32728|6|Mentioned|p16|||See also Fig.14||||||
6698|Fitzmaurice Group|33076|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6698|Fitzmaurice Group|33093|4|Described|Table 2|||||||||
6698|Fitzmaurice Group|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6698|Fitzmaurice Group|33377|6|Mentioned|Table 1|||Re stratigraphy||||||
6698|Fitzmaurice Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6698|Fitzmaurice Group|37462|4|Described|Table 4.VI|||See also p253.||||||18-SEP-06
6698|Fitzmaurice Group|37579|5|Briefly described|Regional setting map legend|Adelaidean|Adelaidean|Sandstone, shale, siltstone, dolomite, conglomerate.||||||10-OCT-05
6698|Fitzmaurice Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6698|Fitzmaurice Group|39563|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6698|Fitzmaurice Group|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6698|Fitzmaurice Group|39801|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, shale, siltstone, dolomite, conglomerate.||||||04-OCT-05
6698|Fitzmaurice Group|39827|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6698|Fitzmaurice Group|40168|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, shale, siltstone, dolomite, conglomerate.||||||18-OCT-05
6698|Fitzmaurice Group|40223|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, shale, siltstone, dolomite, conglomerate.||||||18-MAY-15
6698|Fitzmaurice Group|40494|4|Described|p11|||||||||
6698|Fitzmaurice Group|40495|6|Mentioned|p12|||||||||
6698|Fitzmaurice Group|40764|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6698|Fitzmaurice Group|40765|6|Mentioned|p3|||||||||
6698|Fitzmaurice Group|40808|6|Mentioned|Fig.4|||||||||
6698|Fitzmaurice Group|40809|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6698|Fitzmaurice Group|40823|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
6698|Fitzmaurice Group|41304|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|||||||
6698|Fitzmaurice Group|41305|6|Mentioned|Fig.4|||||||||
6698|Fitzmaurice Group|41407|6|Mentioned|Map legend|Neoproterozoic||||||||
6698|Fitzmaurice Group|41586|6|Mentioned|Map legend|||||||||
6698|Fitzmaurice Group|41645|4|Described|p15|||||||||
6698|Fitzmaurice Group|41646|6|Mentioned|Map legend|Mesoproterozoic||Sandstone, siltstone, shale, conglomerate.||||||17-OCT-05
6698|Fitzmaurice Group|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone, shale, conglomerate.||||||07-OCT-05
6698|Fitzmaurice Group|41661|6|Mentioned|Fig.5|||||||||
6698|Fitzmaurice Group|41980|6|Mentioned|Table 3 P575|||||||||
6698|Fitzmaurice Group|43187|5|Briefly described|p2|||||||||
6698|Fitzmaurice Group|43595|6|Mentioned|p444|||||||||
6698|Fitzmaurice Group|44155|6|Mentioned|p250|||||||Correlated with Carr Boyd Group in WA.||
6698|Fitzmaurice Group|45112|3|Fully described|p53|||p53-58.||||||18-SEP-06
6698|Fitzmaurice Group|45140|6|Mentioned|p13-14|||Kimberley region. Age range given as ?1200-?900 Ma.||||||
6698|Fitzmaurice Group|46675|5|Briefly described|Map legend for regional setting...|Paleozoic|Neoproterozoic|Sandstone, shale, siltstone, dolomite, conglomerate.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
6698|Fitzmaurice Group|46864|5|Briefly described|p40|||||||||
6698|Fitzmaurice Group|47047|6|Mentioned|p220|||||||||
6698|Fitzmaurice Group|48938|4|Described|p13|||||||||
6698|Fitzmaurice Group|48942|3|Fully described|p32|||||||||
6698|Fitzmaurice Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria River Basin.||||||07-FEB-11
6698|Fitzmaurice Group|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Includes: Moyle River Formation, Goobaieri Formation, Lalngang Sandstone, Legune Formation. Sandstone, siltstone, conglomerate.||||||23-JUL-04
6698|Fitzmaurice Group|60526|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Sandstone, shale, siltstone, dolomite, conglomerate.||||||
6698|Fitzmaurice Group|60682|4|Described|piii|Mesoproterozoic|Mesoproterozoic|Thickness: >3500m. Age: ~1200Ma. Silica cemented quartz sandstone and conglomerate. Geological Province: Halls Creek Orogen.||||||
6698|Fitzmaurice Group|60685|6|Mentioned|p2 Fig. 1|||||||||
6698|Fitzmaurice Group|63866|5|Briefly described|p106, p108, p117, p123|||Litchfield Province, Pine Creek Orogen.|||Includes the Moyle River Formation.|Overlain by the Auvergne Group. Intruded by the Ti-Tree Granophyre.||
6698|Fitzmaurice Group|64104|6|Mentioned|p75, p76 fig 10|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone. Suggested source of sedimentary clasts in Duerdin Group in Keep River area.||||||
6698|Fitzmaurice Group|64677|6|Mentioned|p13|||Pine Creek Orogen.|||Moyle River Formation.|||
6698|Fitzmaurice Group|64698|4|Described|lithinterp table|||Age of formations stated to be ~1150-1250Ma (Stenian), but age name given is Statherian? Victoria - Birrindudu Basin, also shown as Halls Creek Orogen. Includes Goobaieri Formation, Lalngang Formation, Moyle River Formation.||||||07-JAN-09
6698|Fitzmaurice Group|65331|5|Briefly described|Map legend + overview geology map legend|Mesoproterozic|Mesoproterozic|?Halls Creek Orogen. Includes Legune Formation, Lalngang Sandstone, Goobaieri Formation, Moyle River Formation. Sandstone, siltstone, conglomerate, shale||||||
6698|Fitzmaurice Group|65339|6|Mentioned|p5 Fig.4. ||||||||Siltstone, shale, sandstone.|
6698|Fitzmaurice Group|65417|5|Briefly described|p158 Fig.2, p159, pp162-163.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone.|||Includes Moyle River, Goobaieri and Legune Formations and Lalngang Sandstone.|||
6698|Fitzmaurice Group|67167|5|Briefly described|Map legend.|||Areas with different magnetic responses are indicated.|||Includes Moyle River, Goobaieri and Lalngang Formations.|||
6698|Fitzmaurice Group|67186|5|Briefly described|Map legend.||||||Includes Moyle River Formation.|||23-NOV-11
6698|Fitzmaurice Group|68733|6|Mentioned|p177, p177 Fig.2|||Victoria Basin. Does not crop out in this study area.||||||05-DEC-17
6698|Fitzmaurice Group|69417|5|Briefly described|p2:5-6|Calymmian|Statherian|Fitzmaurice Basin. More than 3km thick. Is lithostratigraphically similar to the Carr Boyd Basin in adjacent regions of WA.|||||Sandstone-dominated succession.|12-JUL-16
6698|Fitzmaurice Group|69422|6|Mentioned|p7:1-2|||Fitzmaurice Basin. Formerly included as part of the Halls Creek Orogen by Dunster et al. (2000).||||||12-JUL-16
6698|Fitzmaurice Group|69432|6|Mentioned|p17:1|||Dunster et al. (2000) and Cutovinos et al. (2002) did not assign these strata to any Basin. This study assigns them to the newly defined Fitzmaurice Basin.||||||12-JUL-16
6698|Fitzmaurice Group|69435|5|Briefly described|p20:1-3, 5-6|?Mesoproterozoic|Paleoproterozoic|Fitzmaurice Basin (new name, used formally herein). Probably over 3,500m thick. There are no unequivocal chronostratigraphic ages for the Group. Possible correlatives include the Speewah, Kimberley, Carr Boyd, Birrindudu and Limbunya Groups. In the south, the Group is offset by hundreds of metres by the Cockatoo Fault System.|||Moyle River, Goobaieri, Legune Formations; Lalngang Sandstone.||A succession of unmetamorphosed siliciclastic, dominantly arenaceous, sedimentary rocks.|12-JUL-16
6698|Fitzmaurice Group|69673|6|Mentioned|p3 fig 2, p58, p59, p60 fig 48|Mesoproterozoic|Paleoproterozoic|3500m thick. Deposited in alluvial fan, fluvial and shallow marine shelf environments.|||Includes Moyle River Formation, Goobaieri Formation, Lalngang Sandstone, Legune Formation||Arenaceous sedimentary rock.|
6698|Fitzmaurice Group|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.|||Includes Legune Formation, Lalngang Sandstone, Goobaieri Formation, Moyle River Formation.|||
6698|Fitzmaurice Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
6698|Fitzmaurice Group|73083|6|Mentioned|p16|Mesoproterozoic|Mesoproterozoic|||||||
6726|Flamingo Group|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 16|Early Cretaceous|Late Jurassic|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
6726|Flamingo Group|12466|5|Briefly described|p177 Fig.10.|||||||Overlies Plover Formation. Is overlain by Bathurst Island Formation.||03-SEP-14
6726|Flamingo Group|13194|5|Briefly described|p385 Tb. 4-16, p396 fig 4-60|Cretaceous|Oxfordian|60-1500m thick.||||Overlies Troughton Group (unconformably).||
6726|Flamingo Group|13224|5|Briefly described|p484|Berriasian|Kimmeridgian|||||||
6726|Flamingo Group|13234|5|Briefly described|p250 Fig.2,p260,p263 Tb.4,p264.  |Early Cretaceous|Late Jurassic|Has reservoir facies and some oil generation potential: described as early mature for oil.|||Includes the Frigate Shale and Sandpiper Sandstone.|Overlies Plover Formation. Is overlain by Bathurst Island Group.|Includes marine sandstones, shales.|
6726|Flamingo Group|13267|6|Mentioned|pp274-278.|Early Cretaceous|Early Cretaceous|Lower Valanginian.||||Overlies Elang Formation. Is overlain by Echuca Shoals Formation.||
6726|Flamingo Group|22663|5|Briefly described|NT97 -1-4 Fig.3|Cretaceous|Jurassic|||||||01-MAR-10
6726|Flamingo Group|23376|4|Described|p229 Fig.2|Valanginian|Tithonian|Of Bonaparte Basin.||||||18-SEP-06
6726|Flamingo Group|24234|5|Briefly described|p287 Fig.3|Early Cretaceous|Late Jurassic|Geological Province: Bonaparte Basin.||||||
6726|Flamingo Group|24390|5|Briefly described|p3 Table 1|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin.||||||
6726|Flamingo Group|24569|5|Briefly described|p248 Fig. 3|Berriasian|Kimmeridgian|Includes the Frigate Shale and Sandpiper Sandstone.  Geological Province: Petrel Sub-basin.||||||02-MAR-05
6726|Flamingo Group|41459|6|Mentioned|Fig.2|||Reserved as Flamingo Shale Member.||||||18-SEP-06
6726|Flamingo Group|41532|3|Fully described|p305|||||||||
6726|Flamingo Group|41690|5|Briefly described|p6|||See also p74.||||||18-SEP-06
6726|Flamingo Group|41731|6|Mentioned|Fig.3|||||||||
6726|Flamingo Group|42034|4|Described|Fig.4 P11|||||||||
6726|Flamingo Group|42056|4|Described|p98|||||||||
6726|Flamingo Group|42057|4|Described|p75|||See also p79.||||||18-SEP-06
6726|Flamingo Group|42075|5|Briefly described|Fig.4 P245|||||||||
6726|Flamingo Group|42442|3|Fully described|p25|||||||||
6726|Flamingo Group|42861|5|Briefly described|p3|||||||||
6726|Flamingo Group|43661|6|Mentioned|Fig.3|||||||||
6726|Flamingo Group|43699|5|Briefly described|p3-4|Early Cretaceous|Late Jurassic|||||||
6726|Flamingo Group|43707|5|Briefly described|Fig.3,p4||Jurassic|||||||
6726|Flamingo Group|43739|6|Mentioned|p10||Jurassic|||||||
6726|Flamingo Group|49637|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Includes the Swan Formation, Frigate Shale and Sandpiper Sandstone. See also Fig. 3.||||||07-FEB-11
6726|Flamingo Group|50085|5|Briefly described|p3 Tb. 1|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin.||||||
6726|Flamingo Group|60386|6|Mentioned|p302|Early Cretaceous|Late Jurassic|Bonaparte Basin. ||||||
6726|Flamingo Group|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Includes Frigate Shale and Sandpiper Sandstone.  Age: ~150-~136Ma. Geological Province:  Northern Bonaparte Basin and Petrel Sub-basin.||||||01-MAR-10
6726|Flamingo Group|63062|4|Described|p9 Fig. 9, p34|Early Cretaceous|Middle Jurassic|In Bonaparte Basin - mostly mudstones as open marine strata. Study area equivs.in Arafura/Money Shoal Basins - mostly fine-gr.quartzose, partly glauconitic ssts. interbedded with mudst, minor coal - fluvial, deltaic, shallow marine. Max. thick: 1230m.||||||07-FEB-11
6726|Flamingo Group|64695|6|Mentioned|p265, p266-268 Figs.11-13|||A major vitrinite maturity jump at the base of this unit may have been caused by multiple diatreme intrusions. Appears as Flamingo Shales in Fig.11. Appears as Flamingo Sand in Fig.13.|||||Shales.|
6726|Flamingo Group|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Middle Jurassic|Bonaparte Basin.|||Swan Formation, Frigate Shale.|Unconformably overlies Troughton Group.||14-SEP-17
6726|Flamingo Group|69297|6|Mentioned|p283,  p285, p290|Middle Jurassic|Middle Jurassic|Money Shoal Basin. ||||Unconformably overlies the Plover Formation.|Mostly fine-grained, quartzose, glauconitic sandstones, interbedded mudstones and minor coals.|
6726|Flamingo Group|69451|6|Mentioned|p35:2 Fig.35.2; 35:3 Fig.35.4;|Early Cretaceous|Jurassic|||||||12-JUL-16
6726|Flamingo Group|69452|4|Described|p36:4-5, 8, 15, 21-22, 28|Early Cretaceous|Middle Jurassic|Gunn (1988); equivalent to the Flamingo Shale of Botten and Wulff (1990). Offshore. Deltaic to shallow marine to open marine shelf. Drillhole Jabiru-1A intersected a 57m gross oil column in  the Plover Formation and the basal part of this unit, setting the basis for the Jabiru oil field.|||Elang Formation, Frigate Shale, Sandpiper Sandstone.|Overlies Troughton Group disconformably to unconformably.|Siliciclastic and lesser carbonate rocks.|12-JUL-16
6726|Flamingo Group|69456|4|Described|p40:1-6, 9, 15|Early Cretaceous|Middle Jurassic|Gunn (1988). The offshore Money Shoal Basin sucession is consistently referred to as "Flamingo Group equivalent" (to the Bonaparte Basin succession). Not yet recognised in onshore areas of the Money Shoal Basin. Previously called the Money Shoal Group by Petroconsultants (1989), but the name has been abandoned. Includes rocks previously in the upper part of the Petrel Formation (name abandoned), above an unconformity. 1230m thick offshore. Fluvial, deltaic and shallow-marine depositional environments, deepening to the W. Hosts major hydrocarbon accumulations in the Bonaparte and Browse Basins. Fair to very good petroleum source potential in Money Shoal Basin; claystone-rich intervals could provide hydrocarbon seals.||||Unconformably overlies Troughton Group and Plover Formation. Is overlain unconformably by Bathurst Island Group.|Fine-grained, partly glauconitic quartz sandstone with interbedded mudstone and minor coal.|12-JUL-16
6726|Flamingo Group|69653|6|Mentioned|p6, 8, 10, 14-15|Early Cretaceous|Middle Jurassic|Petrel Sub-basin. Post-Callovian event sediments.|||Elang Formation, Frigate Shale, Sandpiper Sandstone.|Unconformably overlies Troughton Group. Is overlain by Bathurst Island Group.||
6726|Flamingo Group|69673|5|Briefly described|p166 fig 136, p173||||||Includes Elang Formation, Lower Frigate Shale, Cleia Formation, Frigate Shale, Sandpiper Sandstone|Disconformably overlies Troughton Group||
6726|Flamingo Group|70061|5|Briefly described|Petrel Sub-basin; Fig.2, p3|Valanginian|Callovian|See also Regional geology: Figs.6-7, p10-12, p14. Sahul: Fig.2, p1-3. Vulcan: Fig.2. Marine shales form a regional seal, and are also suggested to be the main potential sources of oils reservoired in the Laminaria and Corallina accumulations. In Sahul Syncline has stratigraphic traps, and submarine fans form reservoirs.|||Elang Formation, Frigate Shale (Lower and Upper), Sandpiper Sandstone.|Overlies Troughton Group. Is overlain by Bathurst Island Group.||12-JUL-16
6726|Flamingo Group|70098|5|Briefly described|p18 Fig.4, p19 Fig.5|Early Cretaceous|Late Jurassic|Money Shoal Basin. Shown as Flamingo Group-Troughton Group in Fig.4. Early Cretaceous - Jurassic.|||Flamingo Group, Lower; Flamingo Group, Upper; Darwin Formation|Overlies Troughton Group. Is overlain by Bathurst Island Group.||
6803|Ford Run Plateau Dolerite Basalt|30440|6|Mentioned|Table 8|||||||||
6834|Fortescue Group|22449|6|Mentioned|P29||Archean|||||||07-NOV-08
6834|Fortescue Group|22471|6|Mentioned|26 fig 30|Archean|Archean|Geol province Pilbara||||||07-NOV-08
6834|Fortescue Group|22473|5|Briefly described|p 2||Archean|Age 2.7Ga.  Of the Mount Bruce Supergroup. In the Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|22475|5|Briefly described|p493, Fig.1|Archean|Archean|See also Fig.s 2, 3 and 4||||||07-NOV-08
6834|Fortescue Group|22615|5|Briefly described|p 7||Archean|Age: 2760Ma.||||||07-NOV-08
6834|Fortescue Group|22672|6|Mentioned|P267||Archean|Age of unit is 2.7 Ga||||||07-NOV-08
6834|Fortescue Group|22689|6|Mentioned|137,138 fig 1,141|||Geol province Hamersley Basin. Parent Mount Bruce Supergroup||||||
6834|Fortescue Group|22701|4|Described|p40|Archean|Archean|In the Hamersley Basin. Age: 2690+/- 16 Ma zircon. Overlain by Hamersley Group.||||||07-NOV-08
6834|Fortescue Group|22715|6|Mentioned|fig7,p212,213,217|Archean|Archean|Age: 2770-2680Ma||||||07-NOV-08
6834|Fortescue Group|22716|5|Briefly described|table4 p227|Archean|Archean|Formed lower part of Hamersley Basin succession. Overlain by Hamersley Group.||||||07-NOV-08
6834|Fortescue Group|22717|5|Briefly described|P4, Fig3 P18, P9||Archean|Age of unit is 2200 to 2600 Ma||||||07-NOV-08
6834|Fortescue Group|22837|6|Mentioned|Fig.1 p412|||||||||
6834|Fortescue Group|22953|5|Briefly described|p1,Fig1p3||Archean|Max Age: ca 2.7 Ga.||||||07-NOV-08
6834|Fortescue Group|23045|5|Briefly described|289|||Age 2775 +/- 10 - 2629 +/- 5 Ma.||||||16-JAN-07
6834|Fortescue Group|23046|5|Briefly described|166|||Overlain by Hamersley Group. See also p 177.||||||16-JAN-07
6834|Fortescue Group|23047|5|Briefly described|34|||In the Hamersley Province. Of theMount Bruce Supergroup. Overlain by Hamersley Group.||||||16-JAN-07
6834|Fortescue Group|23134|5|Briefly described|p288|||||||||
6834|Fortescue Group|23205|6|Mentioned|p398|||||||||
6834|Fortescue Group|23206|6|Mentioned|Fig.1||Archean|Age: 2.77 - 2.68Ga.||||||07-NOV-08
6834|Fortescue Group|23244|5|Briefly described|Fig.1,2 p23||Archean|Informally divided. Deposition of "lower Fortescue Group' at ca. 2760Ma. Overall age: 2770 - 2680Ma. of Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23255|5|Briefly described|p46 Fig.3||Archean|Base dated at 2.77Ga. of Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23280|6|Mentioned|p1084,Fig1p1085|||||||||
6834|Fortescue Group|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Mount Bruce Supergroup.||||||
6834|Fortescue Group|23348|5|Briefly described|218 Fig.1|||||||||
6834|Fortescue Group|23354|5|Briefly described|316|||||||||
6834|Fortescue Group|23364|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
6834|Fortescue Group|23416|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. In the Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23484|4|Described|p25|Archean|Archean|Of Mount Bruce Supergroup. Age: c. 2770-2680Ma. Intruded by the Gidley Granophyre. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23536|5|Briefly described|Fig 2 p 429|||||||||
6834|Fortescue Group|23570|3|Fully described|p11|Archean|Archean|Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23575|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Overlain by Hamersley Group.||||||07-NOV-08
6834|Fortescue Group|23583|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|23585|4|Described|p14|Archean|Archean|Age: c.2772-2678 Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23590|5|Briefly described|p6|Archean|Archean|Overlain by Tarcunyah Group.||||||07-NOV-08
6834|Fortescue Group|23594|4|Described|p11|Paleoproterozoic|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23598|4|Described|p12|Archean|Archean|Age: c.2770-2680 Ma. Of Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23612|5|Briefly described|p839|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23743|5|Briefly described|p2 Fig 1|Archean|Archean|Age: c.2770 Ma. Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23745|4|Described|p9|Archean|Archean|See also page 7 Fig 5.||||||07-NOV-08
6834|Fortescue Group|23746|4|Described|p12|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23755|4|Described|p57|Archean|Archean|Age: c.2.7 Ga. See also page 17 Table 1. Of Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|23774|6|Mentioned|p733 table 1|||Of Mount Bruce Supergroup.||||||
6834|Fortescue Group|23780|5|Briefly described|p167|Archean|Archean|||||||07-NOV-08
6834|Fortescue Group|23783|5|Briefly described|p7 Fig. 2|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23784|5|Briefly described|p6|Archean|Archean|Of Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|23789|4|Described|p32|Archean|Archean|Age: c.2770-2680Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23793|4|Described|p38|Archean|Archean|Age: c.2770-2629Ma. Of Mount Bruce Supergroup. Geological Province: Hamersley Basin||||||07-NOV-08
6834|Fortescue Group|23794|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|23807|5|Briefly described|p109|||Geological Province: Pilbara Craton.||||||
6834|Fortescue Group|23813|5|Briefly described|p90 Tb. 1|Archean|Archean|Massive and amygdaloidal basalts, minor pillowed lavas, pyroclastics, sandstone/conglomerate lenses. Age: c.2.76-2.69Ga (U-Pb SHRIMP).  Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23870|6|Mentioned|p224 Fig. 1|||Of Mount Bruce Supergroup.||||||
6834|Fortescue Group|23890|5|Briefly described|p5 Fig.2|||Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|23891|5|Briefly described|p90|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|23895|6|Mentioned|p885 Fig.2, p887 Fig.3|||||||||
6834|Fortescue Group|23936|5|Briefly described|p3|Archean|Archean|Geological Province: Hamersley Province. Age: ca. 2775-2687 Ma.||||||07-NOV-08
6834|Fortescue Group|23956|5|Briefly described|p1264|||Unconformably overlies the Gorge Creek Group. Geological Province: Pilbara Craton.||||||
6834|Fortescue Group|24023|4|Described|p26|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|24024|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
6834|Fortescue Group|24025|4|Described|p13|Archean|Archean|Of Mount Bruce Supergroup.  Geological Province:Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|24041|5|Briefly described|p493 fig.2|Paleoproterozoic|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
6834|Fortescue Group|24046|6|Mentioned|p580|||||||||
6834|Fortescue Group|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Mount Bruce Supergroup.  Geological Province: Hamersley Basin||||||07-NOV-08
6834|Fortescue Group|24169|5|Briefly described|p666 Fig. 5|||||||||
6834|Fortescue Group|24183|5|Briefly described|p2 Fig.1, p6, p20|Paleoproterozoic|Archean|Unconformably overlain by the Collier Group.||||||07-NOV-08
6834|Fortescue Group|24184|5|Briefly described|p709, p696, p706 Fig.7|Archean|Archean|of the Mount Bruce Supergroup. Geological Province: Hamersley Basin||||||07-NOV-08
6834|Fortescue Group|24185|5|Briefly described|p734 Fig.1, p744 Tb.4|Archean|Archean|Geological Province:  Hamersley Province.||||||07-NOV-08
6834|Fortescue Group|24188|5|Briefly described|p789 Fig.2, p799|Archean|Archean|Age: <2780 Ma. Geological Province: Hamersley Basin||||||07-NOV-08
6834|Fortescue Group|24189|5|Briefly described|p802 Fig.1, p803|Archean|Archean|Age: 2770-2680 Ma. Geological Province: Mallina Basin.||||||07-NOV-08
6834|Fortescue Group|24190|6|Mentioned|p820 Fig.1|||||||||
6834|Fortescue Group|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Hamersley Basin. Age: 2.77 Ga. Intruded by the Cooya Pooya Dolerite and Gidley Granophyre.||||||07-NOV-08
6834|Fortescue Group|24194|5|Briefly described|p905|Archean|Archean|Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|24203|5|Briefly described|p292 Fig. 7|||Age: <2770 Ma.   Geological Province Carnarvon Basin.||||||
6834|Fortescue Group|24231|6|Mentioned|p186 Fig.2|||Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|24352|5|Briefly described|Map legend|Archean|Archean|Of the: Mount Bruce Supergroup. Age: 2760-2717Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|24353|3|Fully described|p1, 21|Archean|Archean|Underlain by Cherratta Granitoid Complex (unconformable). Age: c.2770-2630Ma. Of the Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|24391|5|Briefly described|p8-2|Archean|Archean|Age: 2.77-2.6 Ga (Arndt et al., 1991). Overlies Lizard hills Formation. Geological Province: Pilbara Block.||||||07-NOV-08
6834|Fortescue Group|24426|6|Mentioned|p240|||||||||07-FEB-11
6834|Fortescue Group|24531|5|Briefly described|p35|Paleoproterozoic|Paleoarchean|Of the Mount Bruce Supergroup.  Age: 2775+/-10Ma.  See also p8-9 Fig. 3.||||||07-NOV-08
6834|Fortescue Group|24532|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup.  Age: 2764-2756Ma.||||||07-NOV-08
6834|Fortescue Group|24533|5|Briefly described|p9, 4 Table 1|Archean|Archean|Lowest unit in the Mount Bruce Supergroup. Predominantly basaltic rocks extending across the Pilbara Craton. Unconformably overlies the Yule Granitoid Complex. Age: c.2775-2630Ma. Geological Province: Hamersley Basin/Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|24534|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup.  Age: 2770-2686Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|24541|2|Defined|p11 Tb.2, p13, p47|Paleoproterozoic|Neoarchean|Geological Province: Hamersley Basin. Age: c. 2770 - 2630 Ma. Unconformably overlies all units of the West Pilbara Granite-Greenstone Terrane.  Conformably overlain by the Hamersley Group. Of the Mount Bruce Supergroup.||||||23-DEC-09
6834|Fortescue Group|24543|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup.||||||23-DEC-09
6834|Fortescue Group|24544|4|Described|p6|Archean|Archean|Lowest unit of Mount Bruce Supergroup. Overlain by Hamersley Group. Age: 2765-2687 Ma. Terrigenous sediments and mafic volcanic rocks. Extensively intruded by mafic sills. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|24550|5|Briefly described|p38, p74 Tb. 5.1.|Archean|Archean|Basalt, rhyolite, sandstone. Age: 2760-2690Ma. Geological Province: Pilbara Craton. See also p158 Fig. 7.12a.||||||07-FEB-11
6834|Fortescue Group|24554|4|Described|p1, p4, p12|Proterozoic|Archean|Of the Mount Bruce Supergroup. Age: c. 2770-2630 Ma. Unconformably overlies granite-greenstone terrane. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|24573|6|Mentioned|p670 Fig.1|||Geological Province: Pilbara Craton||||||
6834|Fortescue Group|24587|5|Briefly described|p54|Archean|Archean|Age: 2.7Ga.  Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Includes: Mount Roe Basalt, snd Hardey, Kylena, Tumbiana and Maddina Formations. Age: ca.2.77Ga. Geological Province: Pilbara Craton. See also p28 Fig. 1.2.||||||07-FEB-11
6834|Fortescue Group|29358|6|Mentioned|p944|||||||||
6834|Fortescue Group|29596|6|Mentioned|p1215|||||||||
6834|Fortescue Group|29629|5|Briefly described|p899|||||||||
6834|Fortescue Group|29716|4|Described|Table 1|||||||||
6834|Fortescue Group|29845|6|Mentioned|p1215|||||||||
6834|Fortescue Group|29848|6|Mentioned|p413|||||||||
6834|Fortescue Group|30096|6|Mentioned|p74|||Stratigraphy||||||
6834|Fortescue Group|30363|6|Mentioned|p10|||||||||
6834|Fortescue Group|30364|6|Mentioned|Fig.1|||||||||
6834|Fortescue Group|30484|6|Mentioned|Fig.29|||||||||
6834|Fortescue Group|30488|6|Mentioned|p91|||Geochronological data||||||
6834|Fortescue Group|30489|6|Mentioned|p96|||Proterozoic age||||||
6834|Fortescue Group|30490|6|Mentioned|p108|||||||||
6834|Fortescue Group|30566|6|Mentioned|p1|||Refers Williams (1968)||||||
6834|Fortescue Group|30766|6|Mentioned|p5|||Lowest units of Nullagine Series||||||
6834|Fortescue Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
6834|Fortescue Group|30882|5|Briefly described|p52|||||||||
6834|Fortescue Group|30955|5|Briefly described|p11|||Formerly named Nullagine||||||
6834|Fortescue Group|31307|6|Mentioned|p80|||Stratigraphy||||||
6834|Fortescue Group|31308|6|Mentioned|p72|||||||||
6834|Fortescue Group|31310|6|Mentioned|p56|||||||||
6834|Fortescue Group|31311|6|Mentioned|p62|||re age dates||||||
6834|Fortescue Group|31392|6|Mentioned|p4|||||||||
6834|Fortescue Group|31393|6|Mentioned|Pl.25|||||||||
6834|Fortescue Group|31670|4|Described|p911|||||||||
6834|Fortescue Group|31671|6|Mentioned|p9|||||||||
6834|Fortescue Group|31819|6|Mentioned|p80|||part of Mt. Bruce Supergroup||||||
6834|Fortescue Group|31828|6|Mentioned|p37|||Map. Proterozoic||||||
6834|Fortescue Group|31853|6|Mentioned|p58|||||||||
6834|Fortescue Group|31876|6|Mentioned|p11|||||||||
6834|Fortescue Group|32144|6|Mentioned|p116|||Solvent extractable organic matter||||||
6834|Fortescue Group|32389|6|Mentioned|p925|||||||||
6834|Fortescue Group|32532|6|Mentioned|p817|||||||||
6834|Fortescue Group|32722|6|Mentioned|Fig.2|||Stromatolite||||||
6834|Fortescue Group|32727|6|Mentioned|Fig.17|||||||||
6834|Fortescue Group|32817|6|Mentioned|p468|||||||||
6834|Fortescue Group|32954|6|Mentioned|p179|||||||||
6834|Fortescue Group|33538|5|Briefly described|p288|||||||||
6834|Fortescue Group|33540|5|Briefly described|p890|||||||||
6834|Fortescue Group|33541|6|Mentioned|p103|||||||||
6834|Fortescue Group|33542|6|Mentioned|p411|||||||||
6834|Fortescue Group|33543|5|Briefly described|p132|||||||||
6834|Fortescue Group|33544|5|Briefly described|p30|||L.Prot.||||||
6834|Fortescue Group|33545|5|Briefly described|p112|||||||||
6834|Fortescue Group|33630|6|Mentioned|Table 1|||||||||
6834|Fortescue Group|33687|6|Mentioned|Fig.1|||||||||
6834|Fortescue Group|33849|6|Mentioned|p124|||||||||
6834|Fortescue Group|34066|5|Briefly described|p4|||L.Prot.||||||
6834|Fortescue Group|34128|6|Mentioned|p17|||||||||
6834|Fortescue Group|34129|6|Mentioned|p57|||Proterozoic||||||
6834|Fortescue Group|34135|5|Briefly described|Table 1|||See also Table 2, pp7,10,11,22. Lower Proterozoic.||||||16-JAN-07
6834|Fortescue Group|34287|6|Mentioned|p32|||Prot. See also P53||||||
6834|Fortescue Group|34834|6|Mentioned|p212|||||||||
6834|Fortescue Group|35025|6|Mentioned|p142|||||||||
6834|Fortescue Group|35084|6|Mentioned|p277|||||||||
6834|Fortescue Group|35176|6|Mentioned|p12|||||||||
6834|Fortescue Group|35218|6|Mentioned|p3|||||||||
6834|Fortescue Group|35260|4|Described|p3|||||||||
6834|Fortescue Group|35269|6|Mentioned|p310|||||||||
6834|Fortescue Group|35523|6|Mentioned|p61|||||||||
6834|Fortescue Group|35583|6|Mentioned|p155|||||||||
6834|Fortescue Group|35641|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6834|Fortescue Group|35681|6|Mentioned|p18|||||||||
6834|Fortescue Group|35949|6|Mentioned|Fig.8|||||||||
6834|Fortescue Group|35975|6|Mentioned|Fig.37|||||||||
6834|Fortescue Group|35976|6|Mentioned|p107|||Also mentioned throughout paper.||||||
6834|Fortescue Group|36003|5|Briefly described|p1027|||||||||
6834|Fortescue Group|36091|5|Briefly described|p572|||||||||
6834|Fortescue Group|36247|6|Mentioned|p186|||See also Fig.2.||||||
6834|Fortescue Group|36257|6|Mentioned|p29|||||||||
6834|Fortescue Group|36258|6|Mentioned|p48|Proterozoic||Geological province: Hamersley Basin.||||||12-MAR-08
6834|Fortescue Group|36308|6|Mentioned|p202|||||||||
6834|Fortescue Group|36551|6|Mentioned|Table 23|||||||||
6834|Fortescue Group|36642|6|Mentioned|Table 1|||||||||
6834|Fortescue Group|36873|5|Briefly described|p27|||||||||
6834|Fortescue Group|36874|6|Mentioned|p84|||||||||
6834|Fortescue Group|36880|6|Mentioned|p108|||||||||
6834|Fortescue Group|36881|5|Briefly described|p114|||||||||
6834|Fortescue Group|36882|3|Fully described|p124|||||||||
6834|Fortescue Group|36891|5|Briefly described|p440|||||||||
6834|Fortescue Group|36902|6|Mentioned|p13|||||||||
6834|Fortescue Group|37212|6|Mentioned|p10|||||||||
6834|Fortescue Group|37297|6|Mentioned|p93|||||||||
6834|Fortescue Group|37299|6|Mentioned|Fig.1|||||||||
6834|Fortescue Group|37327|6|Mentioned|p389|||||||||
6834|Fortescue Group|37371|6|Mentioned|Fig.6.2|||||||||
6834|Fortescue Group|37372|6|Mentioned|p2|||||||||
6834|Fortescue Group|37460|3|Fully described|p111|||||||||
6834|Fortescue Group|37564|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
6834|Fortescue Group|37577|6|Mentioned|p6|||||||||
6834|Fortescue Group|37633|6|Mentioned|p46|||||||||
6834|Fortescue Group|37704|6|Mentioned|p507|||||||||
6834|Fortescue Group|37708|6|Mentioned|Fig.2|||||||||
6834|Fortescue Group|37934|6|Mentioned|Fig.1|||||||||
6834|Fortescue Group|38242|6|Mentioned|p201|||||||||
6834|Fortescue Group|38243|6|Mentioned|Fig.2|||||||||
6834|Fortescue Group|38321|6|Mentioned|Table 1|||||||||
6834|Fortescue Group|38461|6|Mentioned|p1582|||||||||
6834|Fortescue Group|38496|5|Briefly described|p37|||||||||
6834|Fortescue Group|38542|6|Mentioned|p361|||||||||
6834|Fortescue Group|38763|6|Mentioned|p108|||||||||
6834|Fortescue Group|38768|6|Mentioned|p81|||||||||
6834|Fortescue Group|38776|5|Briefly described|Table 1|||||||||
6834|Fortescue Group|38790|6|Mentioned|Table 1|||||||||
6834|Fortescue Group|38988|6|Mentioned|p5|||See also Fig.1||||||
6834|Fortescue Group|39030|6|Mentioned|p2|||||||||
6834|Fortescue Group|39200|4|Described|p279|||||||||
6834|Fortescue Group|39210|3|Fully described|p43|||See also Table 1.||||||14-APR-08
6834|Fortescue Group|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6834|Fortescue Group|39426|4|Described|p10|||||||||
6834|Fortescue Group|39444|6|Mentioned|p6|||||||||
6834|Fortescue Group|39644|6|Mentioned|p4|||||||||
6834|Fortescue Group|39672|6|Mentioned|Fig.2|||||||||
6834|Fortescue Group|39697|3|Fully described|p115|||||||||
6834|Fortescue Group|39837|4|Described|p257|||||||||
6834|Fortescue Group|39894|5|Briefly described|Fig.1|||||||||
6834|Fortescue Group|40081|5|Briefly described|p27|||||||||
6834|Fortescue Group|40089|6|Mentioned|p174|||||||||
6834|Fortescue Group|40103|6|Mentioned|p197|||||||||
6834|Fortescue Group|40105|6|Mentioned|p316|||||||||
6834|Fortescue Group|40255|6|Mentioned|p311|||||||||
6834|Fortescue Group|40369|3|Fully described|p7|||||||||
6834|Fortescue Group|40839|4|Described|p230|||||||||
6834|Fortescue Group|40852|5|Briefly described|p22|||||||||
6834|Fortescue Group|40904|6|Mentioned|p85|||||||||
6834|Fortescue Group|40905|6|Mentioned|p70|||||||||
6834|Fortescue Group|40933|6|Mentioned|p1|||||||||
6834|Fortescue Group|40937|6|Mentioned|p27|||||||||
6834|Fortescue Group|40938|6|Mentioned|p8|||||||||
6834|Fortescue Group|40987|6|Mentioned|Table 2|||||||||
6834|Fortescue Group|41125|6|Mentioned|p55|||||||||
6834|Fortescue Group|41250|5|Briefly described|Table 1|||||||||
6834|Fortescue Group|41263|6|Mentioned|Fig.1|||||||||
6834|Fortescue Group|41349|6|Mentioned|p2|||||||||
6834|Fortescue Group|41351|6|Mentioned|Fig.2|||||||||
6834|Fortescue Group|41354|5|Briefly described|p90|||||||||
6834|Fortescue Group|41355|6|Mentioned|p111|||||||||
6834|Fortescue Group|41357|5|Briefly described|p123|||||||||
6834|Fortescue Group|41358|6|Mentioned|p144|||||||||
6834|Fortescue Group|41592|6|Mentioned|p12|||||||||
6834|Fortescue Group|41594|6|Mentioned|p30|||||||||
6834|Fortescue Group|41635|5|Briefly described|p17|||||||||
6834|Fortescue Group|41669|3|Fully described|p19|||||||||
6834|Fortescue Group|41678|6|Mentioned|p30|||||||||
6834|Fortescue Group|41768|5|Briefly described|p22|||See also p33.||||||16-JAN-07
6834|Fortescue Group|41843|6|Mentioned|p67|||||||||
6834|Fortescue Group|41845|6|Mentioned|p81|||||||||
6834|Fortescue Group|41892|6|Mentioned|p316|||||||||
6834|Fortescue Group|41912|5|Briefly described|p18|||||||||
6834|Fortescue Group|41938|6|Mentioned|p11|||||||||
6834|Fortescue Group|41956|6|Mentioned|p248|||||||||
6834|Fortescue Group|41957|5|Briefly described|p67|||||||||
6834|Fortescue Group|41971|6|Mentioned|Fig.1 P342|||||||||
6834|Fortescue Group|41982|6|Mentioned|Fig.11 P1796|||||||||
6834|Fortescue Group|42013|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
6834|Fortescue Group|42020|5|Briefly described|p316|||||||||
6834|Fortescue Group|42092|4|Described|p143|||||||||
6834|Fortescue Group|42112|4|Described|p6|||See also Fig.1||||||
6834|Fortescue Group|42148|6|Mentioned|Table 1 P687|||||||||
6834|Fortescue Group|42190|5|Briefly described|p273|||||||||
6834|Fortescue Group|42260|5|Briefly described|p6|||||||||
6834|Fortescue Group|42277|5|Briefly described|p63|||||||||
6834|Fortescue Group|42329|5|Briefly described|p3|||See also Fig.1 p4.||||||16-JAN-07
6834|Fortescue Group|42342|5|Briefly described|p20|||Age: 2800-2600 Myr.||||||16-JAN-07
6834|Fortescue Group|42352|5|Briefly described|p4|||||||||
6834|Fortescue Group|42435|6|Mentioned|Fig.1 P43|||||||||
6834|Fortescue Group|42471|4|Described|p4|||Age: 2765-2687 Ma.||||||16-JAN-07
6834|Fortescue Group|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
6834|Fortescue Group|42704|5|Briefly described|Plate 1 and Plate 2E|Archean|Archean|Comprises Mount Roe Basalt, bellary Formation, Hardey Sandstone and Jeerinah Formation.  Age: c. 2750Ma.||||||07-NOV-08
6834|Fortescue Group|42707|5|Briefly described|map legend|Archean||||||||07-NOV-08
6834|Fortescue Group|42708|5|Briefly described|Plate 1|Archean||||||||07-NOV-08
6834|Fortescue Group|42730|5|Briefly described|p5|||||||||
6834|Fortescue Group|42743|5|Briefly described|map legend|Archean||||||||07-NOV-08
6834|Fortescue Group|42744|4|Described|p3|||||||||
6834|Fortescue Group|42785|3|Fully described|p262, Fig.3 p264|Archean|Archean|Of the Mount Bruce Supergroup. Age between 2765Ma and 2684Ma.||||||07-NOV-08
6834|Fortescue Group|42840|5|Briefly described|p289|||||||||
6834|Fortescue Group|42898|5|Briefly described|Fig.2 P341|||of the Mount Bruce Supergroup.||||||16-JAN-07
6834|Fortescue Group|43037|5|Briefly described|p25|||Of the Mount Bruce Supergroup.||||||16-JAN-07
6834|Fortescue Group|43052|5|Briefly described|Fig.3.8|||||||||
6834|Fortescue Group|43055|4|Described|p12|||See also Table 4||||||
6834|Fortescue Group|43056|5|Briefly described|Map Legend|||||||||22-DEC-09
6834|Fortescue Group|43057|5|Briefly described|p61|||||||||
6834|Fortescue Group|43063|5|Briefly described|Fig.1,p48|||||||||
6834|Fortescue Group|43115|6|Mentioned|p178|||||||||
6834|Fortescue Group|43119|4|Described|p4|||Period of deposition 2765-2687 Ma.||||||
6834|Fortescue Group|43210|5|Briefly described|p1,p3.||Archean|||||||07-NOV-08
6834|Fortescue Group|43262|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6834|Fortescue Group|43290|3|Fully described|p4,p18.||Archean|Of the Mount Bruce Supergroup. Age 2765-2687 Ma.||||||07-NOV-08
6834|Fortescue Group|43561|6|Mentioned|p1433|||2765-2687 Ma||||||
6834|Fortescue Group|43595|5|Briefly described|p75,fig.2-48,p218-9|||Age: approx. 2.8 Ga||||||
6834|Fortescue Group|43597|5|Briefly described|p716|||Age: 2765 Ma (U-Pb)||||||
6834|Fortescue Group|43652|6|Mentioned|p390|||||||||
6834|Fortescue Group|43689|6|Mentioned|Fig3p166|||||||||
6834|Fortescue Group|43698|6|Mentioned|p3||Archean|Late Archaean||||||07-NOV-08
6834|Fortescue Group|43756|6|Mentioned|Fig.1,p534|||||||||
6834|Fortescue Group|43821|5|Briefly described|map legend|Archean|Archean|Of Mount Bruce Supergroup||||||07-NOV-08
6834|Fortescue Group|43822|5|Briefly described|map legend|Archean|Archean|Of Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|44141|6|Mentioned|p304|||||||Is overlain unconformably by Bresnahan Group.||
6834|Fortescue Group|44142|6|Mentioned|p323|||||||Is overlain unconformably by Coondoon Formation (Manganese Subgroup).||
6834|Fortescue Group|44150|5|Briefly described|p132 Fig.2-131, p136-137||||2.8-2.7 Ga.|Mount Bruce Supergroup|Mount Roe, Kylena Basalts; Hardey, Tumbiana Formations.|||
6834|Fortescue Group|44151|5|Briefly described|p158, p160 Fig.2-146, p162, p163||||2750 Ma.|||Is overlain by Hamersley Group.||
6834|Fortescue Group|44152|4|Described|p163-191|||MacLeod et al. (1963). Difficulties in correlating scattered outcrops of this unit are discussed.|>2760 Ma.|Mount Bruce Supergroup||Is conformably overlain by Hamersley Group.|Mafic volcanic and volcaniclastic rocks; subordinate acid volcanics, sandstone, conglomerate and carbonate.|
6834|Fortescue Group|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
6834|Fortescue Group|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6834|Fortescue Group|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Mount Bruce Supergroup.  Age: c.2772-c.2687||||||07-NOV-08
6834|Fortescue Group|44438|14|Not recorded|map legend||Paleoproterozoic|Part of Mount Bruce Supergroup. L.Proterozoic inc, Mt.Jope Volcanics. - Jeerinah Formation.||||||07-NOV-08
6834|Fortescue Group|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6834|Fortescue Group|44477|4|Described|p.7-9, Table 1||Proterozoic|SF/50-6.||||||
6834|Fortescue Group|44478|14|Not recorded|map legend||Proterozoic|||||||
6834|Fortescue Group|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
6834|Fortescue Group|44492|14|Not recorded|p.8|||(F50-1,2).||||||
6834|Fortescue Group|44501|14|Not recorded|p.6,11, table 2, map||Paleoproterozoic|(ref. to MacLeod et al 1963, Kreiwaldt 1964). (F50-7). See also p.12,13,16,27,39, for more details. Early Proterozoic.||||||07-NOV-08
6834|Fortescue Group|44502|14|Not recorded|map legend||Proterozoic|||||||
6834|Fortescue Group|44503|4|Described|p.8,9,19,tb.2, map|||Roy Hill Sheet. (F50-12).||||||
6834|Fortescue Group|44504|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
6834|Fortescue Group|44536|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
6834|Fortescue Group|44692|4|Described|p.6,9-11,23,25|||(F50-11).||||||
6834|Fortescue Group|44729|5|Briefly described|map legend|Proterozoic||Of Mount Bruce Supergroup.||||||
6834|Fortescue Group|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6834|Fortescue Group|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6834|Fortescue Group|44867|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
6834|Fortescue Group|45086|4|Described|p22|||Age. Lithology. Iron ore deposits.||||||
6834|Fortescue Group|45965|14|Not recorded|p.58,61|||||||||
6834|Fortescue Group|46319|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|46917|6|Mentioned|p172|||||||||
6834|Fortescue Group|50131|6|Mentioned|p3|Early Proterozoic|Archaean|Of Mount Bruce Supergroup. Includes 8 units and members. Geological Province: Pilbara Craton.||||||22-APR-09
6834|Fortescue Group|50146|5|Briefly described|Map Legend|Archean|Archean|Of the Mount Bruce Supergroup. Geological Province: Hamersley Basin||||||07-NOV-08
6834|Fortescue Group|50189|4|Described|p19|Archean|Archean|Of the Mount Bruce Supergroup. Unconformably overlies Chimingadgi Trondjhemite. Age: 2770-2678Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|50216|5|Briefly described|p209||Archean|Lowest unit within the Mount Bruce Supergroup. Consists of metsedimentary rocks and metabasalts, variably intruded by dolerite sills. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|50217|5|Briefly described|p220, p221 Fig.1|Archean|Archean|Age: 2775-2629 Ma (Arndt et al, 1991; Nelson et al, 1999). Geological Province: Hamersley Province (Pilbara Craton). See also p232.||||||07-NOV-08
6834|Fortescue Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
6834|Fortescue Group|50227|6|Mentioned|p443 Fig. 1|||Age: 2900-<2800Ma.  See also p444 Tb. 1, p447 Fig. 3||||||07-FEB-11
6834|Fortescue Group|50287|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Mount Bruce Supergroup.  Geological Province: Hamersley Basin.  Includes: Mount Roe Basalt, Hardey Formation, Kylena Formation, Tumbiana Formation, Maddina Formation.||||||07-NOV-08
6834|Fortescue Group|50370|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|50381|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|50382|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|50423|5|Briefly described|p215, Fig.1, p216||Archean|Unconformably overlies southern part of Shaw Granitoid Complex. East Pilbara Granite-Greenstone Terrane.||||||07-NOV-08
6834|Fortescue Group|50427|4|Described|p174 Fig.1|Archean|Archean|Age: <=2770 Ma. Unconformably overlies De Grey Group. Flood basalts. Of Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|50544|4|Described|p43, p10 Fig. 5|Neoarchean|Neoarchean|Of the Mount Bruce Supergroup. Overlies the Grergory Granite Complex and unconformably overlies the Gorge Creek Group Group; disconformably overlain by the Carawine Dolomite (Hamersley Group).  Age: c.2775-2629Ma (Nelson et al, 1999).  Geol.Prov:  Hamersley Basin||||||12-JUN-14
6834|Fortescue Group|50549|5|Briefly described|p1158|Paleoproterozoic|Archean|Of the Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|50555|5|Briefly described|Map legend|Archean|Archean|Includes the Jeerinah, Maddina, Tumbiana, Kylena and Hardey Formations, and Mount Roe Basalt.  Geological Province: Hamersley Basin.||||||23-DEC-09
6834|Fortescue Group|60112|5|Briefly described|p105, p107 Fig.1, p108-119.  |||Hamersley Province. Some of the youngest rocks of the Pilbara Craton. Timing of deformation is discussed.|<2775 Ma||Includes Mount Roe, Glen Herring Creek, and Pear Creek, Sequences.|Unconformably overlies the Warrawoona Group/Pilbara Supergroup.|Includes flood basalts.|
6834|Fortescue Group|60362|5|Briefly described|p1517, p1534|Archean|Archean|Compositional similarities with Louden and Mount Negri Volcanics.|c.2.7 Ga.||||Includes massive outpourings of basaltic magma.|
6834|Fortescue Group|60373|4|Described|p144, p145 Tb. 1, p148, p152|Archean|Archean|Of Mount Bruce Supersequence. Includes Jeerinah, Maddina, Tumbiana, Kylena and Hardey Formations and Mount Roe Basalt. Age: 2775 - 2684Ma. Geological Province: Hamersley Province.||||||
6834|Fortescue Group|60429|4|Described|p2, p19|Archean|Archean|Of Mount Bruce Supergroup. Comprises Mount Roe Basalt, Hardey, Kylena, Tumbiana, Maddina and Jeerinah Formations. Unconformably overlies Warrawagine Granitoid Complex. Age: 2772-2687Ma. Geological Province: Hamersley Basin. See also p8 Fig. 4.||||||07-FEB-11
6834|Fortescue Group|60636|6|Mentioned|p34 Fig. 3.1|||||||||07-FEB-11
6834|Fortescue Group|60706|5|Briefly described|p622|||Basal epiclastic unit of the Mount Bruce Supergroup. Conformably overlain by the Hamersley Group. Max. thickness: ~7km. Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|61111|6|Mentioned|p96 Fig.2|||||||||30-SEP-15
6834|Fortescue Group|61205|5|Briefly described|p548|||Geological Province: Pilbara Craton. Overlies Gorge Creek Group. Siliciclastic sediments.||||||31-MAY-07
6834|Fortescue Group|61252|6|Mentioned|p64|||||||||
6834|Fortescue Group|61253|5|Briefly described|p54-55 Fig. 3|Neoarchean|Neoarchean|Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61254|5|Briefly described|p256-p258|Neoarchean|Neoarchean|Up to 5000m thick.|||Includes the Tumbiana, Maddina and Jeerinah Formations.|Is overlain by Hamersley Group.|Succession of mafic and felsic volcanics and associated sedimentary rocks.|
6834|Fortescue Group|61257|5|Briefly described|p354 Fig. 1|Archean|Archean|Geological Province: North Pole Dome of the Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61259|5|Briefly described|p403|Archean|Archean|Max. age: 2851+/-2Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61264|5|Briefly described|p64 Fig. 2|||Of the Mount Bruce Supergroup.||||||17-MAY-06
6834|Fortescue Group|61265|4|Described|p43|Archean|Archean|Includes the Mount Roe Basalt and the Kylena, Maddina, Tumbiana and Hardey Formations. Thickness: 2-3km. Unconformably overlies the Pilbara granite-greenstone terrane. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61266|5|Briefly described|p55, p58 Tb.1, p61|Archean|Archean|Geolgocial Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61267|6|Mentioned|p72|||||||||
6834|Fortescue Group|61268|5|Briefly described|p78 Fig.1|||Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||
6834|Fortescue Group|61276|6|Mentioned|p577 Fig.1|||||||||
6834|Fortescue Group|61575|5|Briefly described|p759|||Includes the Jeerinah Formation. Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|61576|5|Briefly described|p774 Fig. 1|||Includes the Jeerinah Formation. ||||||
6834|Fortescue Group|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|61579|5|Briefly described|p59 Fig. 3, p60|Archean|Archean|Age: ~2700Ma. See also p61 Fig. 5. ||||||07-NOV-08
6834|Fortescue Group|61847|5|Briefly described|p295, p297 Fig. 4|Archean|Archean|Metasediments and metavolcanics. Overlie the Hamersley Group unconformably. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|62094|5|Briefly described|p236|Archean|Archean|Includes the Maddina Basalt. Geological Province: Hamersley Basin. See also the informal Fortescue group.||||||07-NOV-08
6834|Fortescue Group|62129|4|Described|p2, p4, p5-6, p13 Fig. 1, p17, p21, p23|Archaean|Archaean|Of Mount Bruce Supergroup. Includes six units. Age: 2765 - 2687Ma. Geological Province: Hamersley Basin.||||||07-FEB-11
6834|Fortescue Group|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes seven units. Geological Province: Hamersley Basin, Pilbara Craton.||||||23-MAR-09
6834|Fortescue Group|62427|6|Mentioned|p2 Fig.1|||||||||
6834|Fortescue Group|62576|5|Briefly described|p618 Fig. 1, p620 Fig. 3|Archean|Archean|Age: 2775-2630Ma. Geological province: Pilbara Craton. Three distinct types of conglomerate have been mapped in this group (lithological details included on p622-623). ||||||07-NOV-08
6834|Fortescue Group|62579|5|Briefly described|p116, p118|Archean|Archean|Of the Mount Bruce Supergroup. Age: 2.7Ga. Max. thickness 500m. Stromatolite occurrences in the Hamersley district - in chert, carbonate, basalt and tuff. Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|62979|5|Briefly described|p212 Fig. 1|Archean|Archean|Age: 2780-2630Ma. Geological Province: Pilbara Craton.||||||07-FEB-11
6834|Fortescue Group|63139|5|Briefly described|p50|||Of the Mount Bruce Supergroup. In east Pilbara. Comprises mostly terrigenous clastic sedimentary rocks with lesser shales and mafic and felsic volcanic rocks.||||||29-MAR-07
6834|Fortescue Group|63142|5|Briefly described|p487 Fig. 2|||Includes Mount Roe Basalt.  Geological Province: Warrawoona Syncline.||||||
6834|Fortescue Group|63153|5|Briefly described|p1359, p1361 Fig.2, p1362 Fig.3|Neoarchean|Neoarchean||2.8-2.6 Ga (Richards and Blockley, 1984).|Of the Mount Bruce Supergroup.|Includes Jeerinah Formation.|Conformably underlies the Hamersley Group.|Thick volcanogenic and minor clastic and chemical sedimentary rock units.|
6834|Fortescue Group|63245|5|Briefly described|p4 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
6834|Fortescue Group|63367|4|Described|p229-247. |Neoarchean|Neoarchean|Hamersley Basin, Pilbara Craton. This article argues for a lacustrine or very shallow lagoonal, not marine, environment of deposition for the stromatolitic carbonates in the Tumbiana Formation.|2.78-2.63 Ga|Lower part of the Mount Bruce Supergroup.|Includes the Mount Roe Basalt; Kylena, Boongal, Maddina, Bunjinah, Hardey, Tumbiana, Pyridie and Jeerinah Formations.|Overlain by the Hamersley Group.|Succession of flood basalts and interbedded sedimentary formations, up to 7 km thick.|
6834|Fortescue Group|63372|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin. Of the Mount Bruce Supergroup.||||||07-NOV-08
6834|Fortescue Group|63417|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Comprises Mount Roe Basalt, Hardey, Kylena, Tumbiana, Maddina and Jeerinah Formations and the Gregory Range Suite and Black Range Dolerite Suite. Geological Province: Fortescue Basin.||||||07-NOV-08
6834|Fortescue Group|63420|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Includes Bellary Formation, Mount Roe Basalt, Hardey and Pear Creek Formations.  Age ranges: c.2775Ma, c. 2764-2756Ma and c.2741Ma. Geological Province: Marble Bar Sub-basin/Hamersley Basin.||||||07-NOV-08
6834|Fortescue Group|63432|5|Briefly described|p735 Fig. 1, p736 Fig. 2|Archean|Archean|Includes the Jeerinah Formation.||||||07-FEB-11
6834|Fortescue Group|63441|5|Briefly described|p17 Fig. 4, p25 Fig. 7|Neoarchean|Neoarchean|Unconformably overlies Lalla Rookh Sandstone. Age: 2775-2630Ma. Geological province: Pilbara Craton/East pilbara terrane. See also p31-34Figs. 10, 11, 12 and 13.||||||07-FEB-11
6834|Fortescue Group|63538|5|Briefly described|p1, p3 Fig. 2|Archaean|Archaean|Age: 2770 - 2630 Ma. Geological Province: De Grey Superbasin.||||||17-APR-13
6834|Fortescue Group|63854|5|Briefly described|p229 Fig.2, p233.|Neoarchean|Neoarchean|Hamersley Basin.||Of the Mount Bruce Supergroup.|Includes Maddina Formation.|Unconformably overlies Black Range Dolerite Suite and Bridget Suite.||
6834|Fortescue Group|63866|5|Briefly described|p144, p162|Paleoproterozoic|Archaean|Hamersley Basin.||Mount Bruce Supergroup|Includes the Kylena Formation.|Unconformably overlain by the Collier Group.||
6834|Fortescue Group|64174|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Represented by undivided basaltic and sedimentary rocks in this area.||||||07-NOV-08
6834|Fortescue Group|64326|5|Briefly described|p70|Archean|Archean|Top of Mount Bruce Supergroup. Represents flood basalt province that erupted onto older basement rocks of Pilbara Craton. Two contrasting interpretations of the stratigraphy are presented. Age: 2.77-2.63Ga.Geol.prov: Hamersley Basin/Marble Bar Sub-basin||||||07-FEB-11
6834|Fortescue Group|64328|5|Briefly described|p53|Archean|Archean|Age: 2770-2630Ma.||||||07-FEB-11
6834|Fortescue Group|64384|4|Described|p23, p29-36, p51|Archean|Archean|Of Mount Bruce Supergroup - of 12 named stratigraphic units in northern Pilbara Craton + southern Hamersley Basin. Age at base: c.2765Ma (Arndt et al in press). Mafic volcanic-dominated rocks. See also p48 Fig. 40.||||||07-FEB-11
6834|Fortescue Group|64405|5|Briefly described|p2 Fig. 1|Archean|Archean|Geological province: Fortescue Basin.||||||07-FEB-11
6834|Fortescue Group|64573|5|Briefly described|p784|||Overlian by Hamersley Group. Geological Province: Pilbara Craton. Volcanic and clastic sedimentary rocks.||||||07-FEB-11
6834|Fortescue Group|64580|4|Described|map legend||Neoarchean|Of Mount Bruce Supergroup. Basaltic and sedimentary rocks.||||||09-DEC-08
6834|Fortescue Group|64621|5|Briefly described|Map legend|Archean|Archean|Of Mount Bruce Supergroup.  Contains Bellary, Hardey, Kylena and Pear Creek Formations and Mount Roe Basalt.||||||07-NOV-08
6834|Fortescue Group|64628|6|Mentioned|p171 Fig.1. |||||||||
6834|Fortescue Group|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes five units with three members. Geological Province: Pilbara Craton.||||||07-FEB-11
6834|Fortescue Group|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes Jeerinah, Maddina, Tumbiana, Kylena and Hardey Formations. Age: c. 2766Ma - c. 2629. Geological Province: Pilbara Craton (Hamersley Basin).||||||17-NOV-08
6834|Fortescue Group|64656|5|Briefly described|Map Legend|Archaean|Archaean|Includes Kylena, Tumbiana, Maddina and Jerrinah Formations. Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes Hardey, Tumbiana, Maddina and Jeerinah Formations. Geological Province: Hamersley Basin.||||||
6834|Fortescue Group|64662|5|Briefly described|p44|Archean|Archean|Age: ~2.78Ga (Nelson 1999). Pilbara Craton. Possible source rocks for Ferdies Member, Dead Bullock Formation.||||||07-FEB-11
6834|Fortescue Group|64722|5|Briefly described|Fig. 2 p3-6, p7, 23|Neoarchean|Neoarchean|Hamersley Basin succession from rifting of the Pilbara and Yilgarn cratons in the late Archean / early Proterozoic. Overlies Pilbara Craton.||||Overlain by Hamersley Group.||11-APR-12
6834|Fortescue Group|64724|4|Described|p42 Fig. 3|Neoarchean|Neoarchean|Hamersley Basin.|||Contains Mount Roe, Kylena and Maddina Basalts; Hardey, Boongal, Pyradie, Tumbiana, Bunjinah and Jeerinah Formations.|||02-APR-12
6834|Fortescue Group|64725|6|Mentioned|p59.|||||||||
6834|Fortescue Group|64728|6|Mentioned|p94 Fig.1, p97, p107.||||Depositional age from c.2780 Ma to c.2629 Ma.|||Is overlain by Hamersley Group.||
6834|Fortescue Group|64747|6|Mentioned|p94 fig 1, p95 fig 2, p96|||||||||
6834|Fortescue Group|64936|5|Briefly described|map legend|Archean|Archean|Of Mount Bruce Supergroup. Includes Pear Ceek Formation, Kylena Formation, Hardey Formation, Black Range Dolerite suite, Mount Roe Basalt and Bellary Formation. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
6834|Fortescue Group|65008|5|Briefly described|p5, p7, p8, p11, p13-17, p21, p22, p41|Neoarchean|Neoarchean|Hamersley Basin. Oldest component of the Mount Bruce Supergroup. |2775-2629 Ma|Of the Mount Bruce Supergroup.|Includes Maddina Formation, Tumbiana Formation, Kylena Formation, Hardey Formation, Black Range Dolerite Suite, and Mount Roe Basalt.|Unconformably underlain by the De Grey Group, Wyman Formation, Mosquito Creek Formation, and Charteris Basalt.||
6834|Fortescue Group|65194|5|Briefly described|p98 Fig.4.23|||Unit in Mount Bruce Supergroup.||||||11-APR-16
6834|Fortescue Group|65415|6|Mentioned|p119 Fig.1.|||||||||
6834|Fortescue Group|65506|6|Mentioned|p987 Fig.1A|||||||||
6834|Fortescue Group|65683|5|Briefly described|p799, p800 Fig1, p801 Fig 2,|||Of Mount Bruce Supergroup. Underlies Marra Mamba Iron Formation of the Hamersley Group; includes Jeerinah Formation.||||||08-MAR-12
6834|Fortescue Group|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Includes Jeerinah Formation, Maddina Formation, Tumbiana Formation, Kylena Formation, Hardey Formation and Mount Roe Basalt. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
6834|Fortescue Group|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Of Mount Bruce Supergroup. |Includes Maddina, Tumbiana, Kylena and Hardey Formations; Mount Roe Basalt and Black Range Dolerite suite.|||
6834|Fortescue Group|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin.||Of Mount Bruce Supergroup. |Includes Maddina, Tumbiana, Kylena and Hardey Formations and Mount Roe Basalt.|||
6834|Fortescue Group|65757|6|Mentioned|p81 Tb.2|||In the Hamersley Basin. Includes Jeerinah Formation.||||||
6834|Fortescue Group|65825|4|Described|p1, p4, pp6-7, pp20-23. |Neoarchean|Neoarchean|Hamersley Basin. Referred to as the Nullagine and Mount Jope Supersequences by Blake and Barley (1992). A thick sequence of mafic and felsic volcanic rocks and related sedimentary rocks. Outcrop area is a dissected plateau, with scattered remnants of deeply weathered rock capped by ferruginous duricrust. Deposition of its upper sediments is interpreted to have occurred on a thermally subsiding continental margin. Cut by numerous faults.|Deposition 2775 - 2629 Ma.|Unit in Mount Bruce Supergroup.|Includes Kylena, Maddina, Jeerinah, Hardey and Tumbiana Formations; and Mount Roe Basalt.|Is overlain conformably by Carawine Dolomite.||
6834|Fortescue Group|65827|3|Fully described|p1-2,p5,p7-8,p12 Tb.3,p21,p28,p32-41|Neoarchean|Neoarchean|Of Mount Bruce Supergroup; previously of Nullagine Series.  c.2772-2713 Ma. Includes basal Mount Roe Basalt, Hardey Formation. Unconformably overlies Mount Edgar Granitic Complex, Gorge Creek Group, Pilbara Supergroup, Charteris Basalt, Wyman Formation, Apex Basalt; intruded by Round Hummock Dolerite Suite. Mis-spelt as Fortescue group in Tb.3. Mafic volcanic and sedimentary rocks.||||||
6834|Fortescue Group|65828|6|Mentioned|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Unit in Mount Bruce Supergroup.|Includes Mount Roe Basalt; Hardey, Kylena, Tumbiana, Maddina and Jeerinah Formations.|||
6834|Fortescue Group|65829|3|Fully described|p5, p7 Fig.3, pp14-23. |Neoarchean|Neoarchean|A thick volcanic and sedimentary rifting succession. All its rocks dip away from the underlying Yilgalong Granitic Complex, which was a topographic high during deposition of this Group. Their deposition ended a c.500 m.y. hiatus of weathering and erosion of the East Pilbara Terrane following the intrusions of the Cleland Supersuite into the Yilgalong Granitic Complex. The mixed lithologies outcrop as ranges and strike-controlled ridges; the mainly basaltic rocks form rugged hills with dendritic drainage.|2.77 - 2.63 Ga.|Unit in Mount Bruce Supergroup.|Includes Mount Roe Basalt; Hardey, Kylena, Tumbiana, Maddina and Jeerinah Formations.|Overlies unconformably the Pilbara Supergroup and Yilgalong Granitic Complex. Is disconformably overlain by the Carawine Dolomite.||
6834|Fortescue Group|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin. Of Mount Bruce Supergroup. Includes Bellary, Hardey (with its Bamboo Creek Member), Kylena, Tumbiana, Maddina (with its Kuruna Member) and Pear Creek Formations; Mount Roe Basalt; and an unnamed dolerite or gabbro dyke or sill.||||||11-APR-13
6834|Fortescue Group|66115|6|Mentioned|p137 Fig.1|||||||||
6834|Fortescue Group|66118|5|Briefly described|p148 Fig.2, p150, p153 Fig.7, p158|||Pilbara Craton. East Pilbarra Terrane.|c. 2780-2630 Ma|Mount Bruce Supergroup||Unconformably overlies rocks in the northern margin of Pilbara Well greenstone belt.||
6834|Fortescue Group|66217|4|Described|p1, p2, p6, p10, p14, pp37-39, pp44-55.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Ages from Arndt et al. (1991), Trendall et al. (2004), and others. Up to 6.5 km thick. Deposited over 200,000 km2, but outcrops over 40,000 km2.|2775-2630 Ma.|Basal unit in Mount Bruce Supergroup.|Includes Bellary, Hardey, Kylena, Tumbiana, Maddina, Boongal, Pyradie, Bunjinah, Jeerinah and Pear Creek Formations and Mount Roe Basalt.|Unconformably overlies Warrawoona and Croydon Groups and Shaw Granitic Complex. Is conformably overlain by Hamersley Group.|Interbedded volcanic and clastic sedimentary rocks.|
6834|Fortescue Group|66574|6|Mentioned|p912, p913|||Mount Bruce Supergroup. Underlies the Hamersley Group. Records rifting of Archean Pilbara Craton c.2775 Ma. Hydrothermal alteration at 2466-2063 Ma.||||||
6834|Fortescue Group|66664|6|Mentioned|p3, p4, p5, p8, p9.|||Fortescue Basin.|||Includes Mount Roe Basalt.|||
6834|Fortescue Group|66685|4|Described|p215-7, p226, p229, p234|Archean|Archean|Pilbara Craton. Thorne and Trendall, 2001. >6500m thick, thickening north to south. Regionally metamorphosed. Deposited in a continental rift setting. A non-contemporaneous combination of complex packages of subaerial basalts, and fluvial, lacustrine, and ?marine deposits. |2775-2630 Ma||Includes Mount Roe Basalt; Hardey, Kylena,Tumbiana, Maddina and Jeerinah Formations.||Consists of a succession of flood basalts, volcaniclastic sediments, siliciclastic sediments, and carbonates.|
6834|Fortescue Group|66745|6|Mentioned|p50 Fig.1.|Neoarchean|Neoarchean|||Unit in Mount Bruce Supergroup.||||
6834|Fortescue Group|66887|5|Briefly described|p2, p20-21|||Pilbara Craton.|||Mount Roe Basalt, Koongaling volcanics (lower case volcanics is informal use of unit name), Jeerinah Formation|||
6834|Fortescue Group|67025|4|Described|pp318-328.|Archean|Archean|Hamersley Basin, Pilbara Block. Low-grade volcanic and sedimentary rocks, resting unconformably on Archean granite-greenstone basement. The natural remanent magnetisation and mean bulk susceptibility of units in this Group are detailed in this article. There exists a regional remanent magnetic overprint directed moderately upwards to the northwest|2780 - 2629 Ma (Trendall et al. 2004).|Lowest unit in Mount Bruce Supergroup.|Includes Mount Roe and Maddina Basalts, Hardey Sandstone, Mount Jope Volcanics, and Bunjinah and Jeerinah Formations.|Is conformably overlain  by Hamersley Group.||
6834|Fortescue Group|67056|4|Described|p419 Fig.2, pp422-423. |Archean|Archean|Includes several formations with total thickness in excess of 4.5 km.|c.2.77 - 2.63 Ga.|Basal unit in Mount Bruce Supergroup.||Is conformably overlain by Hamersley Group.|Sequence of flood and submarine basalts (in northern and southern areas respectively), with interbedded coarse alluvial fan clastics and minor chemical sediments.|
6834|Fortescue Group|67127|5|Briefly described|p91||||||||Sedimentary and volcanic rocks.|
6834|Fortescue Group|67130|5|Briefly described|p1, p6, p24 fig 17|Neoarchean|Neoarchean|Greater than 6km thick. Flood basalts erupted in three separate events as part of continental rifting. The authors note 2km thick unit of subaerial tholeiitic basalt underneath the accepted part of this unit which could be added to this unit. Sedimentary rocks were deposited in fresh water settings (lacustrine). See also  p49 fig 46, p50 fig 47, p62. |2780 Ma - 2630 Ma|Mount Bruce Supergroup|Includes Tumbiana Formation, Bellary Formation, Mount Roe Basalt, Hardey Formation, Kylena Formation, Maddina Basalt, Jeerinah Formation|Conformably (and gradationally) overlain by Hamersley Group|Subaerial tholeiitic basalts, subordinate pillow basalts, basaltic tuff, felsic volcanics, volcaniclastics, intrusive rocks and clastic sedimentary rocks (conglomerate to shale) with stromatolitic carbonates.|
6834|Fortescue Group|67183|4|Described|p639-640, 642-643, 649, 651-2, 670 |Neoarchean|Neoarchean|Divided into the basal Kylena Basalt and overlying Maddina Basalt (Hickman 1978). Fortescue Group Basalts appears in Fig.3. Includes volcano-sedimentary units. |ca 2775-2715 Ma various sources|Mount Bruce Supergroup|Mount Roe Basalt; Kylena, Maddina, Jeerinah, Tumbiana, Hardey Formations; Marra Mamba Iron Formation.|Conformably overlain by the Hamersley Group.|Includes volcano-sedimentary units, mafic units.|
6834|Fortescue Group|67197|6|Mentioned|p3|||Fortescue Basin.||||||
6834|Fortescue Group|67201|4|Described|p5, p9, p14-15, p19, see comments|Archean|Archean|In northern Pilbara Craton. In west Pilbara, was deposited in Northwest Pilbara Sub-basin. Unconformably overlies Kurrana Terrane. All units comprise Fortescue Basin. Thickness: ~6 km. Predominantly volcanic succession that unconformably overlies Pilbara Craton across 250 000 km2. Basaltic rocks erupted in 3 main events, each lasting no more than 10 m.y. Page location continued: p25, p27-30, p33-38, p44, p49, p51, p53 Fig.40, p62 Fig.52.|2780-2630 Ma|Mount Bruce Supergroup|basal Bellary Formation, Mount Roe Basalt, Hardey Formation, Boongal Formation, Kylena Formation, Pyradie Formation, Tumbiana Formation, Bunjinah Formation, Maddina Formation, top Jeerinah Formation|Unconformably overlies Nickol River Formation. Unconformably overlies Whundo Group. See comments|Undivided basaltic and sedimentary rocks. Continental flood basalts, but basaltic andesite is more widespread. Volcanic rocks in upper part of group are mafic-felsic volcanic cycles in NW of basin.|22-NOV-16
6834|Fortescue Group|67202|4|Described|p16, p51-52, p54, p64, p66, p125|Archean|Archean|See also p231-232, p234, p236, p258, p281. Fortescue Basin. Over 7km thick. Overlies eastern Pilbara Craton. Gently to moderately folded. Considerably disrupted by NNW to N oriented faults. Epithermal base-metal mineralisation dated at 2720-2620 Ma. Poorly magnetised: not readily subdivided using aeromagnetic data. Shown on p258 as including Carawine Dolomite.|||Mount Roe, Kylena Basalts; Hardey, Tumbiana, Jeerinah, Maddina Formations.|Is overlain unconformably by Tarcunyah Group, Waltha Woora Formation and disconformably by Carawine Dolomite.|Basaltic flows with volcaniclastic sediments dominating the lower and upper parts, separated by felsic volcanics.|
6834|Fortescue Group|67229|5|Briefly described|p1-4|Paleoproterozoic|Neoarchean|Fortescue Basin.|2780-2450 Ma.|Mount Bruce Supergroup.|Tumbiana, Pyradie Formations.|Is overlain by the Hamersley and Turee Creek Groups.||
6834|Fortescue Group|67269|5|Briefly described|p5, p20-21 Fig.19|Paleoarchean|Paleoarchean|Pilbara.|||Mount Roe Basalt; Hardey, Kylena, Tumbiana Formations.|||
6834|Fortescue Group|67270|6|Mentioned|p3, p6-7, p12|||Fortescue Basin.|||Mount Roe Basalt.|||
6834|Fortescue Group|67721|5|Briefly described|p37, p38 Fig.9|Neoarchean|Neoarchean||c. 2775-2639 Ma|Of the Mount Bruce Supergroup.||||
6834|Fortescue Group|67829|5|Briefly described|p453.|||Hydrothermal leaching of this unit at depth is suggested (Blake et al. 2011) as source of silica for Pinjian Chert Breccia.||||||
6834|Fortescue Group|67855|5|Briefly described|p211, 212, 224, 225, 227, 229, 231|||Hamersley Basin.||Of Mount Bruce Supergroup.||||
6834|Fortescue Group|67888|6|Mentioned|p51||||||Includes Tumbiana Formation|||
6834|Fortescue Group|68035|4|Described|p291, 294, 283, p284 Fig 1, p286, Fig 6|Neoarchean|Neoarchean|Fortescue Basin. Prior to 2007 included in Pilbara Craton, but now considered to overlie it. Crustal extension and volcanic plateau volcanism. 6 km thick. Includes a recently developed important lode Au deposit, Paulsens.|2780-2630 Ma||Includes Bellary Formation, Black Range Dolerite, Mount Roe Basalt, Hardey Formation, Kylena Formation, Tumbiana Formation, Maddina Formation, Jeerinah Formation.|Overlies Pilbara Craton.|Predominantly volcanic succession.|
6834|Fortescue Group|68056|5|Briefly described|p169-171, 175, 188, 190-191|Archean|Archean|Pilbara Craton. Up to 5,000m thick. Has not been affected by intense deformation or metamorphism.|||Tumbiana, Maddina, Mount Roe, Kylena, Hardey, Jeerinah Formations.||Mafic and felsic volcanic and sedimentary rocks.|
6834|Fortescue Group|68101|5|Briefly described|p1-3, p6, p10|Neoarchean|Neoarchean|Fills the Fortescue Basin. Deposition in multiple sedimentary environments.|||Includes Kylena, Boongal, Maddina, Jeerinah and Tumbiana Formations.||Volcanic, volcaniclastic, siliciclastic and carbonate sedimentary rocks. Dominantly flood basalts; lesser fossiliferous sedimentary rocks.|
6834|Fortescue Group|68280|6|Mentioned|p1, p2 fig 1a, p3, p5, p19, p32, p54|Paleoproterozoic|Neoarchean||2780-2630 Ma||Includes Jeerinah Formation, Maddina Formation, Tumbiana Formation, Kylena Formation, Hardey Formation, Mount Roe Basalt, Black Range Dolerite Suite, Mount Jope Volcanics|||
6834|Fortescue Group|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|c.2775-2735 Ma.|Of the Mount Bruce Supergroup.|Includes Kylena Formation, Hardey Formation, Mount Roe Basalt, Bellary Formation.|||02-DEC-14
6834|Fortescue Group|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2766-2715 Ma|Of the Mount Bruce Supergroup|Includes Tumbiana Formation, Hardey Formation.|||03-DEC-14
6834|Fortescue Group|68283|5|Briefly described|Map Legend|Archean|Archean|Marble Bar Sub-basin, Fortescue Basin.||Of the Mount Bruce Supergroup.|Includes Pear Creek Formation, Kylena Formation, Hardey Formation, Mount Roe Basalt, Bellary Formation.|||23-SEP-13
6834|Fortescue Group|68284|6|Mentioned|p4|||Crops out in the Marble Bar-Nullagine area, East Pilbara Terrane.|2775-2630 Ma.|||||
6834|Fortescue Group|68312|6|Mentioned|p103|Archean|Archean|North Pole Dome, Pilbara Craton.|<2.8 Ga.|||||
6834|Fortescue Group|68574|6|Mentioned|p2-3|||||||||
6834|Fortescue Group|68981|5|Briefly described|p21, p26|Paleoproterozoic|Archean|Pilbara Craton. Overlies Archean granite-greenstone terranes. Volcanic and sedimentary rocks. Detrital zircons discussed.||||||
6834|Fortescue Group|69003|6|Mentioned|p7, p9 Fig.9, p27, p36|||During the 2215-2145 Ma Ophthalmia Orogeny, this unit was deformed, folded, and thrust northward over the Pilbara Craton to form the Ophthalmia Fold Belt.|2775-2630 Ma.|||||
6834|Fortescue Group|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.||Of the Mount Bruce Supergroup.|Includes Tumbiana, Kylena and Hardey Formations, and Mount Roe Basalt.|||29-APR-14
6834|Fortescue Group|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|||Includes Tumbiana Formation, Kylena Formation, Hardey Formation, and Mount Roe Basalt.|||
6834|Fortescue Group|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Dated by Rasmussen et al. (2005), and Arndt et al. (1991). See map legend for a detailed lithological description.|||Includes Jeerinah, Bunjinah, Pyradie, Boongal, Hardey and Bellary Formations, and Mount Roe Basalt.|||06-MAY-14
6834|Fortescue Group|69041|6|Mentioned|p8|||Pilbara Craton.||||Unconforably overlies the Chimingadgi Trondhjemite.||
6834|Fortescue Group|69080|4|Described|p684, p686-687, p690-699, p701|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Thickness to 6.5 km in South Pilbara Sub-basin. The seven constituents are grouped into four tectono-stratigraphic units. Thick mafic to ultramafic sills intrude much of the succession above Mount Roe Basalt. Deposition in an extensional tectonic setting. Hosts significant gold deposits in association with the Nanjilgardy Fault.|c.2775-c.2629 Ma (Trendall et al., 2004).||Bellary Formation; Mount Roe Basalt; Hardey Formation; Boongal, Pyradie and Bunjinah Formations; Jeerinah Formation.|Is overlain conformably by Hamersley Group.|Basalt, basaltic andesite and felsic volcanic rocks with locally thick siliciclastic sedimentary rocks; local carbonate rocks; komatiitic basalt and dolerite sills.|
6834|Fortescue Group|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean||||Includes Bellary Formation, Hardey Formation, Jeerinha Formation, Boongal Formation, Pyradie Formation, Mount Roe Basalt.||Basalt, dolerite dykes or layered sills; coarse grained pyroxenite overlain by leucocratic gabbro or dolerite; local basal serpentinite; metamorphosed.|
6834|Fortescue Group|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Mount Bruce Supergroup|Includes Jeerinah Formation, Pear Creek Formation, Maddina Formation, Tumbiana Formation, Kylena Formation, Hardey Formation, Mount Roe Basalt, Bellary Formation||Sandstone, pebbly sandstone and coarse grained sandstone;minor pebble conglomerate; thickly bedded. Metagabbro and metadolerite; sheared. Dolerite or gabbro dykes or sills.|
6834|Fortescue Group|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Hamersley Basin. Also includes Kylena Formation, Maddina Formation, Mount Roe Basalt, Pyradie Formation, Tumbiana Formation. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.||Unit of Mount Bruce Supergroup.|Includes Bellary Formation, Boongal Formation, Bunjinah Formation, Cooya Pooya Dolerite, Hardey Formation, Jeerinah Formatio.||Layered sills; coarse-grained pyroxenite overlain by leucocratic gabbro or dolerite dykes and sills; local basal serpentinite; metamorphosed|
6834|Fortescue Group|69299|3|Fully described|p1-2, p4-5, p7, p9, p12-17, p19-21, map|Neoarchean|Neoarchean|Landscape formations form rocky dissected plateau, and large areas are without soil cover. Outcrops or shallow subcrops on about 98% of COOYA POOYA. Hickman(1983) recognized 8 formations of volcanic alternating with dominantly sedimentary formations. Kojan and Hickman (1998) argued that two distinct mafic-felsic volcanic cycles are present within the redefined Maddina Basalt of Thorne and Tyler (1997a). These cycles coincide with previously recognised Kylena Basalt and Maddina Basalt, and that andesite and dacite are widespread in upper parts of Kylena and Maddina Basalts, and therefore renamed these as Kylena Formation and Maddina Formation. Thorne and Trendall (2001, p220) described Fortescue Group lavas as basaltic andesite, and parts of Kylena Formation and Maddina Formation are andesite, dacite, and rhyolite. On COOYA POOYA, all rocks are remetamorphosed to prehnite-pumpellyite facies (Smith et al. 1982).|c. 2770-2630 Ma|Oldest group within Mount Bruce Supergroup.|Includes Mount Roe Basalt, Hardey Formation, Kylena Formation, Cooya Pooya Dolerite, Tumbiana Formation, Maddina Formation.|Unconformably overlies Whundo Group, Cherratta Granitoid Complex and Mallina Basin; overlies De Grey Group.|Continental succession of volcanic and sedimentary rocks.|
6834|Fortescue Group|69300|5|Briefly described|map legend|Archean|Archean|Hamersley Basin.|c.2770-2630Ma Arndt et al 1991; Nelson et al 1992||||undivided basalt, dolerite, andesite, sandstone, and shale|
6834|Fortescue Group|69301|4|Described|p2, p4 Fig.2, p16-19, p21 Fig.8, p23|Neoarchean|Neoarchean|Pilbara Craton. Entire Fortescue Basin. Thickness: 6 km. Spans 150 million years (2.78-2.63 Ga). Basaltic formations (that distinguish this group from the conformably overlying Hamersley Group) were erupted in three mafic-felsic volcanic cycles, each lasting no more than 10 million years. The dominantly volcanic part of the group can be divided into three depositional sequences (Mount Roe Basalt, Hardey Formation, and Kylena to Maddina Formations), each of which represents a separate stage in the evolution of the depositional basin. Jeerinah Formation (upper part of Fortescue Group), is assigned to sequence 4, which also includes Hamersley Group.|2775-2630 Ma|Mount Bruce Supergroup|Jeerinah Formation, Mount Roe Basalt, Hardey Formation, Kylena Formation, Maddina Formation, Bunjinah Formation, Tumbiana Formation, Pyradie Formation, Boongal Formation|Is conformably overlain by Hamersley Group.|Stromatolites. Predominantly volcanic succession. Basaltic andesite is more widespread than basalt.|
6834|Fortescue Group|69387|6|Mentioned|p6|||Southern Pilbara Craton. Extension-rift fill sequence of siliciclastic sedimentary and volcanic rocks.||||||
6834|Fortescue Group|69411|5|Briefly described|p282,292|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Deposited during period of rifting and extensive volcanism; dominated by flood basalts and also contaisn siliciclastic, volcaniclastic and carbonate units.|2775-2630 Ma|Unit of Mount Bruce Supergroup.|Includes Maddina, Tumbiana and Kylena formations.|Underlain by Paleoarchean basement.||
6834|Fortescue Group|69538|5|Briefly described|p516 Fig.2, p517 Fig.3, p520, p526|Paleoproterozoic|Paleoproterozoic|See also p531, p534, p555, p559 Fig.34, p561, p572, p583-585. |2.77 Ga.|Basal unit in Mount Bruce Supergroup.|Includes Jeerinah Formation.|Is overlain by Hamersley Group.||
6834|Fortescue Group|69563|6|Mentioned|p689-690, p699||||||Includes Jeerinah Formation, Mount Roe Basalt, Maddina Basalt and Kylena Formation.|||25-MAY-16
6834|Fortescue Group|69565|6|Mentioned|p131, p133 Fig.1, p139-140|||Hamersley Province.||Mount Bruce Supergroup.||Is overlain by Hamersley Group.||
6834|Fortescue Group|69566|6|Mentioned|p236-237|||East Pilbara Granite-Greenstone Terrane.|2770-2640 Ma.||||Dominantly volcanic and sedimentary rocks.|
6834|Fortescue Group|69569|6|Mentioned|p285 Figs.1,2; p288|||East Pilbara Terrane.|||Mount Roe Basalt; Kylena, Hardey, Maddina, Tumbiana, Jeerinah Formations.|||
6834|Fortescue Group|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Northeast Pilbara Sub-basin; Marble Bar Sub-basin, Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv2_5m_geologyp98_lut, 500k_interpgeol_lut.csv.|2780-2629 Ma (inferred)|Unit of Mount Bruce Supergroup.|Includes Bellary Formation, Hardey Formation, Jeerinah Formation, Kylena Formation, Maddina Formation, Mount Roe Basalt, Tumbiana Formation.|Intruded by Bridget Suite.|Pebbly sandstone and coarse-grained sandstone; minor pebble conglomerate; thickly bedded; metagabbro and metadolerite; sheared; dolerite or gabbro dyke or sill.|
6834|Fortescue Group|69596|5|Briefly described|p1-2, p4-7, p8 Fig.5, p37|Archean|Archean|Ophthalmia Fold Belt, Capricorn Orogen. Up to 6km thick.|2775-2630 Ma.|||Is overlain conformably by Hamersley Group.|Dominated by thick mafic and ultramafic successions and abundant siliciclastic sedimentary rocks.|
6834|Fortescue Group|69739|5|Briefly described|p69|||Hamersley Basin.|2.7 Ga.|Mount Bruce Supergroup.|Jeerinah Formation.|Is overlain by Marra Mamba Iron Formation (Hamersley Group).|Mostly mafic igneous rocks.|
6834|Fortescue Group|69745|5|Briefly described|p269-273, 275-281, 283, 287, 290|||Hamersley Province.|c.2.77-2.6 Ga.||Mount Jope Formation, Jeerinah Formation.|Is overlain conformably by Hamersley Group.|Mainly volcanic rocks, including tholeiitic and andesitic basalts, locally pillowed, and dolerites.|
6834|Fortescue Group|69754|6|Mentioned|p315 fig 1|||Pilbara Craton.||||||
6834|Fortescue Group|69792|5|Briefly described|p1095-6, p1099, p1105-07|Neoarchean|Neoarchean|Southern margin of Pilbara Craton.|c.2.78-c.2.63 Ga.||Includes Mount Roe Basalt; Hardey, Kylena, Boongal, Tumbiana, Pyradie, Maddina, Bunjinah and Jeerinah Formations.||A succession of flood basalts and sedimentary rocks.|
6834|Fortescue Group|70086|6|Mentioned|p207|Neoarchean|Neoarchean||||Includes Tumbiana Formation.|||
6834|Fortescue Group|70507|6|Mentioned|p431|Archean|Archean|Geological province: Pilbara Craton.||||||
6834|Fortescue Group|70509|5|Briefly described|p14|Neoarchean|Neoarchean|Geological province: Hamersley Province; Pilbara Craton. Top and bottom geochronological analysis ages includes 2629+\-5 Ma (Trendall et al., 2004) and 2772+\-10 Ma (Arndt et al., 1991) respectively.||||Overlain by Hamerley Group. Underlain by Archean basement.|Flood basalts and rhyolites.|
6834|Fortescue Group|70729|6|Mentioned|p164-165|||Geological province: East Pilbara Terrane, Pilbara Craton. Of Fortescue Basin.||||||
6834|Fortescue Group|70733|6|Mentioned|p105-106|||Eastern Pilbara Craton.|<2775 Ma.||Jeerinah impact layer.|||
6834|Fortescue Group|70775|4|Described|p2, p4, p10, p13, p15-p17|Neoarchean|Neoarchean|Unconformably overlies the Roebourne and Sholl greenstone belts. See also p24, p37, p41, p47, p53-p54, p68, p70-p71, p79-p80, p95-p96.|c. 2775-2629 Ma|Mount Bruce Supergroup|Includes the Mount Roe Basalt.|Overlies the Munni Munni Intrusion. Unconformably overlies the Tarlwa Pool Tonalite and the Bookingarra Group.|Undivided basaltic and sedimentary rocks.|
6834|Fortescue Group|70795|4|Described|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2775-2629 Ma||Includes Jeerinah Formation, Hardey Formation, Bellary Formaton and Mount Roe Basalt.||Dolerite dyke or sill, siliciclastic sedimentary rocks, mafic volcanic rocks, local carbonate rocks, chert, and dolerite sills. Basalt, basaltic andesite, dacite, rhyolite, komatiite, basaltic breccia, siltstone and mudstone.|
6834|Fortescue Group|70814|5|Briefly described|p34-p35|Neoarchean|Neoarchean||2775-2629 Ma|||||
6834|Fortescue Group|70826|6|Mentioned|p2,  p6 Tbl 2, p8|Neoarchean|Neoarchean|Pilbara Craton. Informally subdivided into 5 sequences in Table 2, p6.||||||22-APR-20
6834|Fortescue Group|70884|5|Briefly described|p122-124,133,135|Neoarchean|Neoarchean|Geological province: East Pilbara Terrane, Pilbara Craton. Of Fortescue Basin. Deposited contemporaneously with D5 deformation (oblique strike-slip faulting) along carbonate-altered shear zones and reactivation of greenstone synclines within the East Pilbara Terrane. Associated with Black Range Dyke Swarm.|2.78-2.63 Ga|||||
6834|Fortescue Group|70936|6|Mentioned|p61|Neoarchean|Neoarchean|Geological province: Gascoyne Province, Pilbara Craton.||||||
6834|Fortescue Group|70949|5|Briefly described|p987-989, p998|Archean|Archean|Fortescue Basin, northern Capricorn Orogen. Hosts the Mount Olympus gold deposit. Regional scale metamorphism is synchronous with or post-dates the Ophthalmian Orogeny. Metasomatism discussed.|||||Folded metasediments.|
6834|Fortescue Group|70958|5|Briefly described|p1, 2, Fig. 1, p16|Paleoproterozoic|Paleoproterozoic|May occur as allochthonous rafts in Meteorite Bore Member.|||||Basic igneous rocks with clastic horizons.|
6834|Fortescue Group|71003|6|Mentioned|p61-p62|Archean|Archean|Pilbara Craton.||||||
6834|Fortescue Group|71041|6|Mentioned|p42,43||||2775-2630 Ma.|||||
6834|Fortescue Group|71042|4|Described|p64 fig 1, p65-p66|Archean|Archean|Oakover Basin, Southern Pilbara. See also Arndt et al, 1991 for date. [NB it is unclear whether the author is intentionally reassigning the Marra Mamba Formation to this group or just showing old terminology]. See also p69-p70, p72-p73, p75-p76, p79-p80, p82, p94, p96-p99.|2775 - 2715 Ma (Blake et al, 2004)|Mount Bruce Supergroup|Includes the Jeerinah Formation, Hardey Formation, Maddina Formation, Kylena Formation, Tumbiana Formation.|Conformably overlain by the Carawine Dolomite (Hamersley Group).|Basaltic and volcaniclastic rocks.|24-MAY-19
6834|Fortescue Group|71112|5|Briefly described|p68-70,72,79|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Records start of rifting in the Archean Pilbara Craton.|~2775 Ma|Unit of Mount Bruce Supergroup.||||
6834|Fortescue Group|71137|6|Mentioned|p5|Archean|Archean|At least 620m thick in the Mount Grant area.|||||Widespread lavas and sediments; metagabbro intrusions.|
6834|Fortescue Group|71169|5|Briefly described|p63-p64, p87|Neoarchean|Neoarchean|Fortescue Basin.|2775-2629 Ma||Includes the Bellary Formation, Hardey Formation and the Kylena Formation.|||
6834|Fortescue Group|71267|5|Briefly described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sedimentary rock, basalt, mafic intrusions including dolerite, gabbro|
6834|Fortescue Group|71309|5|Briefly described|p754|||Pilbara Craton. These basalts have near-flat HREE, unlike the Norseman dyke suites in the Kalgoorlie Terrane.|2.76-2.69 Ga.||||Includes continental flood basalts.|
6834|Fortescue Group|71349|6|Mentioned|p736|||||||||
6834|Fortescue Group|71487|5|Briefly described|p128|Archean|Archean|Of Fortescue Basin.||||Underlain by De Grey Supergroup.||
6834|Fortescue Group|71513|6|Mentioned|p66 fig 1,|||Pilbara Craton. Metamorphosed from prehnite to pumpellyite facies to greenschist facies elsewhere.||||Overlain by the Hamersley Group.||
6834|Fortescue Group|71550|6|Mentioned|p36,45|||Geological province: Of Hamersley Basin.|||Includes Jeerinah Formation.|||03-SEP-19
6834|Fortescue Group|71782|14|Not recorded|Plates 7,8||Early Proterozoic|Between p60-61.||||||
6834|Fortescue Group|71803|4|Described|p365-p368, p371, p380-p381, p385-p386|Neoarchean|Neoarchean|Pilbara Craton. Geochemistry discussed. Interpreted to have been deposited in an extensional setting with largely terrestrial to shallow marine conditions.|ca. 2770-2690 Ma|Mount Bruce Supergroup|Includes the Mount Roe Formation, Kylena Formation, Bunjinah-Maddina Formation and the Jeerinah Formation.||Ultramafic to felsic volcanic and associated sedimentary rocks up to 6.5km in thickness.|
6834|Fortescue Group|71808|4|Described|v-vi, p5, p7-p8, p10, p37, p43|||Hamersley Province. Terrestrial to shallow marine. See also p47, p64, p81, p85, p87, p97, p104, p149, p162, p164.|ca 2770-2630 Ma|Mount Bruce Supergroup|Includes the Jeerinah Formation, Bellary Formation, Mount Roe Basalt, Hardey Formation, Kyleena Formation, Boongal Formation, Tumbiana Formation and Maddina Formation.|Conformably overlain by the Hamersley Group.|Mafic volcanic and syn-volcanic dolerite sills with interflow sediments including shales, cherts, carbonates, tuffaceous sediments and shallow marine to deltaic and fluvial sediments.|
6834|Fortescue Group|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Fortescue Basin. Informally subdivided into 4 unnamed units and 5 named sequences.|Max age 2775+/-10 Ma, Min age 2629+/-5 Ma.|Mount Bruce Supergroup|Includes 1.Bellary Formation, Mount Roe Basalt; 2. Hardey Formation; 3. Boongal, Kylena Formations; 4. Pyradie, Pear Creek, Tumbiana, Bunjinah, Maddina Formations; 5. Jeerinah Formation.||Basalt, basaltic andesite, felsic volcanic rocks w local thick siliciclastic sedimentary rocks; local carbonate rocks. Layered mafic/ultramafic sills; pyroxenite; local serpentinite. Metagabbro, metadolerite. Dolerite/gabbro dykes/sills.|
6834|Fortescue Group|72254|6|Mentioned|App.A p10-11|Neoarchean|Neoarchean|Basal unit of the Mount Bruce Supergroup.||Mount Bruce Supergroup||Overlain by Hamersley Group.||
6834|Fortescue Group|72447|6|Mentioned|p238|||||||||
6834|Fortescue Group|72493|5|Briefly described|p28, 30|||Hamersley Basin.|2.78 - 2.69 Ga.|Basal Mount Bruce Supergroup.|Jeerinah Formation.|Is overlain conformably by the Hamersley Group.|Largely volcanic and volcaniclastic rocks.|
6834|Fortescue Group|72569|6|Mentioned|p2|||Of the Hamersley Basin.||Mount Bruce Supergroup||Conformably overlain by the Hamersley Group.||
6834|Fortescue Group|72570|6|Mentioned|p3 fig 1|||||Mount Bruce Supergroup||||
6834|Fortescue Group|72668|5|Briefly described|p9, p10. p16-19, p22|Neoarchean|Neoarchean|Northern Pilbara Craton.|c. 2775-2630 Ma|||Unconformably overlies the Gorge Creek Group and the Croydon Group.||13-JAN-22
6834|Fortescue Group|72705|6|Mentioned|p15-16|||Pilbara Craton. Source of some of the 2.7 -2.5 Ga zircons in the Edmund Group.||||||
6834|Fortescue Group|72712|6|Mentioned|p1, p2, p3, p4, p8, p9, p10, p11.|Neoarchean|Neoarchean|Part of the Turee Creek Basin (Formerly McGrath Trough).|c. 2775+/-10 Ma to 2629+/-5 Ma.|Base of Mount Bruce Supergroup|Jeerinah Formation, Bunjinah Formation, Maddina Formation, Pyradie Formation, Tumbiana Formation, Boongal Formation, Kylena Formation, Hardey Formation, Mount Roe Basalt, Bellary Formation|Shown as overlying deformed granite-greenstone basement. Overlain by Hamersley Group.||
6834|Fortescue Group|72758|4|Described|p3, p5-6, p16-17 Tb.1, p19-22.|Paleoproterozoic|Neoarchaean|This group is the lowermost unit of the Mount Bruce Supergroup. See also p4 Fig.1., p14, p28, p33, p35, p37, p55, p58-59.|Deposition between 2750-2490 Ma|Mount Bruce Supergroup|Includes Mount Roe Basalt, Hardey Sandstone, Mount Jope Volcanics and Jeerinah Formation|Unconformably overlies the Metawandy Granite. Unconformably overlain by Hamersley Group, Wyloo Group.|Consists mainly of mafic lavas and pyroclastics, but includes some felsic volcanics, conglomerate, sandstone, BIF, chert, dolerite, and mudstone.|
6834|Fortescue Group|73022|6|Mentioned|p2, p3 Fig.2|||||Mount Bruce Supergroup|Jeerinah Formation|Underlies the Hamersley Group|Includes organic-rich shale, lesser Fe-chert and minor shale.|
6834|Fortescue Group|73102|6|Mentioned|p2 Fig.1|||||||||
6834|Fortescue Group|73160|6|Mentioned|p2 Fig.1, p6|Neoarchean|Neoarchean||2.77-2.63 Ga|||Unconformably overlies De Grey Supergroup.|Includes dolerite dykes.|
6834|Fortescue Group|73168|6|Mentioned|p762, 765|Neoarchean|Neoarchean|Hamersley Basin. Deposited in a syn-rifting setting.|2775-2630 Ma||||Volcano-sedimentary sequences.|
6834|Fortescue Group|73290|6|Mentioned|p783-784||||||Jeerinah Formation.|||
6834|Fortescue Group|73442|6|Mentioned|p2 Fig.1|||||||||
6834|Fortescue Group|73538|6|Mentioned|p1-5, p7-8|||Interpreted as a sediment source for the overlying Boolgeeda Iron Formation and Turee Creek Group. [The name Fortescue volcanics, p1, may informally refer to a component of this unit]. Weathering of these Late Archean subaerial flood basalts dominated the continental detrital and chemical fluxes to the Hamersley Basin prior to about 2.45 Ga.||Mount Bruce Supergroup|Jeerinah, Maddina, Bunjinah, Pyradie, Tumbiana, Kylena, Boongali, Hardey, Bellary, and Mount Roe Basalt formations|Overlain by Nammudi Member, Marra Mamba Iron Formation, Hamersley Group.|Includes mafic volcanics.|
6834|Fortescue Group|73598|6|Mentioned|p1208-1209|||East Pilbara Terrane.|c.2700 Ma.||Mount Roe Basalt.||Sedimentary and volcanic rocks.|
6834|Fortescue Group|75075|5|Briefly described|p419-420, 426|Neoarchean|Neoarchean|Western Pilbara Craton.|c.2687-2765 Ma (Arndt et al., 1991).|Mount Bruce Supergroup.||Is intruded by Yanyare dykes.|Sedimentary and volcanic rocks.|
6851|Fossil Cliff Member|15881|5|Briefly described|p62|Permian|Permian|Of Holmwood Shale in Irwin and Lockier River valley areas. Formerly named Fossil Cliff Formation (Playford et al 1975), this unit was subsequently placed within the Holmwood Shale as its uppermost section by Playford et al (1976). Contains Ammonoids.||||||12-FEB-09
6851|Fossil Cliff Member|22820|5|Briefly described|p10 Fig.4|Early Permian|Early Permian|Of Holmwood Shale.||||||11-AUG-08
6851|Fossil Cliff Member|23172|4|Described|Map Legend|Permian|Permian|||||||
6851|Fossil Cliff Member|23174|5|Briefly described|Fig5p8,10|Early Permian|Early Permian|||||||
6851|Fossil Cliff Member|23279|5|Briefly described|p13|||Miswritten for Fossil Cliff Limestone Member. (Woolnough and Somerville, 1924).||||||
6851|Fossil Cliff Member|31910|4|Described|Table 1|||See p17.||||||05-NOV-15
6851|Fossil Cliff Member|36257|6|Mentioned|Table 2.1|||||||||
6851|Fossil Cliff Member|36293|6|Mentioned|p100|||||||||
6851|Fossil Cliff Member|37294|6|Mentioned|p104|||||||||
6851|Fossil Cliff Member|37549|6|Mentioned|Fig.4|||||||||
6851|Fossil Cliff Member|38217|6|Mentioned|p269|||||||||
6851|Fossil Cliff Member|39223|6|Mentioned|p238|||||||||
6851|Fossil Cliff Member|39263|6|Mentioned|p152|||||||||
6851|Fossil Cliff Member|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
6851|Fossil Cliff Member|41044|6|Mentioned|p128|||||||||
6851|Fossil Cliff Member|41049|6|Mentioned|p44|||||||||
6851|Fossil Cliff Member|41315|6|Mentioned|p149|||||||||
6851|Fossil Cliff Member|41514|5|Briefly described|p62|||Most recent interpretation by Playford et al (1976) for the Fossil Cliff sequence, previously known as Fossil Hill Formation -- is that this "is best regarded as a member of the Holmwood Shale"  with which it interfingers an which it conformably overlies.||||||18-AUG-08
6851|Fossil Cliff Member|41632|6|Mentioned|p4|||||||||
6851|Fossil Cliff Member|42017|6|Mentioned|p5|||||||||
6851|Fossil Cliff Member|42309|6|Mentioned|p253|||Perth Basin||||||
6851|Fossil Cliff Member|42392|6|Mentioned|p115|||Member of Holmwood Shale||||||
6851|Fossil Cliff Member|42473|6|Mentioned|p7|||of Holmwood Shale||||||
6851|Fossil Cliff Member|42994|6|Mentioned|p36|||of Holmwood Shale||||||
6851|Fossil Cliff Member|43015|5|Briefly described|Table 1,p319|||||||||
6851|Fossil Cliff Member|43018|5|Briefly described|Table 1,p386|||||||||
6851|Fossil Cliff Member|43050|5|Briefly described|p16|||||||||
6851|Fossil Cliff Member|43067|5|Briefly described|Fig.12,p124|||of Holmwood Shale||||||
6851|Fossil Cliff Member|49644|5|Briefly described|Table|||||||||
6851|Fossil Cliff Member|61811|4|Described|p3 Fig.2, pp36-39, p63.|Sakmarian|Sakmarian|Northern Perth Basin. Formerly Fossil Cliff Formation (Clarke et al. 1951); redefined (Johnson et al. 1954 and Playford et al. 1976) to Member status because it is thin, lenticular and difficult to map. Type section at Fossil Cliff on the North Branch of the Irwin River; further details in Appendix 1. Cold-water, richly fossiliferous shallow-marine carbonates.||Uppermost unit in Holmwood Shale.||Is overlain by High Cliff Sandstone.|Interbedded dark micaceous and gypsiferous siltstone, sandy siltstone, shale, and bioclastic calcarenite deposited in a series of coarsening-upward parasequences.|
6851|Fossil Cliff Member|62113|5|Briefly described|p619 Fig.2, p620 Fig.3, p625. |Sakmarian|Sakmarian|At Fossil Cliff, contains a diverse assemblage of plant microfossils, marine macrofossils, foraminifera, ostracoda and algae.||Unit in Holmwood Shale.||||
6851|Fossil Cliff Member|64635|5|Briefly described|p4 Fig.3, p18-19, p22-25      |Sakmarian|Sakmarian|Formerly Fossil Cliff Formation (Clarke et al., 1951). Type section is best exposed at Fossil Cliff, on the North Branch of the Irwin River, immediately upstream from High Cliff. Age is either late Tastubian or Sterlitamakian based on a single specimen of the ammonoid Metalegoceras kayi from the type section (Glenister et al., 1973). Type section diagram p22 Fig.19.||Of the Holmwood Shale.||Overlain by the High Cliff Sandstone.|Consists of interbedded dark micaceous and gypsiferous siltstone, sandy siltstone, shale and bioclastic calcarenite deposited in a series of coarsening-upward parasequences. Richly fossiliferous.|
6851|Fossil Cliff Member|66949|6|Mentioned|p22|||||Unit in Holmwood Shale.||Corelated with Nura Nura Member (Poole Sandstone).||
6851|Fossil Cliff Member|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||Holmwood Shale.||||
6851|Fossil Cliff Member|68297|5|Briefly described|p198|Artinskian|Artinskian|Carnarvon Basin. Includes microvertebrate fossils.||Said to be of Holmswood Shale||||
6851|Fossil Cliff Member|69547|4|Described|p180,182,193,197-198,200|Sakmarian|Sakmarian|northern Perth Basin. Located in the upper section of the Holmwood Shale.||Unit of Holmwood Shale.||Overlain and underlain by Holmwood Shale mudstone.|Discontinuous nodular limestone beds and highly fossiliferous friable sandy mudstones.|
6851|Fossil Cliff Member|73623|5|Briefly described|p5-6, 13-16|Sakmarian|Sakmarian|Irwin Basin. Contains undeformed, very well preserved porcellanous calcitic foraminifera (discussed).||Holmwood Shale|||Friable calcarenite beds in shale succession with indurated nodular limestone. Ammonoids extremely rare.|
6858|Fossil Head Formation|7142|6|Mentioned|p350 Fig.4.|Late Permian|Early Permian|Browse Basin.||||Overlies Kulshill Group. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|12466|5|Briefly described|p173.|||A hydrocarbon extract is a mature light paraffinic crude oil with no overt evidence for biodegradation; sourced from predominantly terrestrial organic matter deposited in estuaries.||||Overlies Keyling Formation. Is overlain by Hyland Bay Formation.||03-SEP-14
6858|Fossil Head Formation|12733|6|Mentioned|p565.|Early Permian|Early Permian|Bonaparte Basin. Gas-prone.||||||
6858|Fossil Head Formation|13194|4|Described|p382, p387, p396, p400, p405.|Kungurian|Artinskian|See Table 4-16, Figures 4-59, 4-60 and 4-71. Type Section: Tern 1 well (2993-3569m). 116-650m thick marine shelf deposits.||Kinmore Group||Overlies Keyling Formation (conformably). Overlain by Hyland Bay Formation.|Siltstone, mudstone, sandstone; minor limestone, and coal.|
6858|Fossil Head Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kinmore Group.||||
6858|Fossil Head Formation|13234|6|Mentioned|p250 Fig.2, p252 Fig.4,p262 Tb.3,  |Permian|Permian|Proven reservoir and seal.||||Overlies Keyling Formation and Kulshill Group. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|13242|5|Briefly described|p214 Fig. 2, p215|Late Permian|Late Permian|Represents the base of Late Permian stratigraphy of the Bonaparte Basin. Formerly underlay Hyland Bay Formation; now underlies the Pearce Formation (Hyland Bay Sub-group). Geological Province: Bonaparte Basin. See also p226 Fig. 8.||||||07-FEB-11
6858|Fossil Head Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Late Permian|Early Permian|Bonaparte Basin. Unit of Kinmore Group. Overlies Kulshill Group and underlies Hyland Bay Formation. Equivalent to Poole Sandstone and Noonkanbah Formation in onshore Canning Basin.||180||||28-OCT-14
6858|Fossil Head Formation|22663|5|Briefly described|NT97 -1-4 p2||Permian|||||||01-MAR-10
6858|Fossil Head Formation|23377|6|Mentioned|p212 Fig.5||Early Permian|Of Vulcan Sub-basin.||||||18-SEP-06
6858|Fossil Head Formation|23820|4|Described|p205|Early Permian|Early Permian|Geological Province: Bonaparte Gulf Basin.||||||
6858|Fossil Head Formation|24378|5|Briefly described|p14|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
6858|Fossil Head Formation|24569|5|Briefly described|p248 Fig. 3|Early Permian|Early Permian|Of the Kinmore Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
6858|Fossil Head Formation|40077|6|Mentioned|Table 1|||||||||
6858|Fossil Head Formation|41532|3|Fully described|p301|||||||||
6858|Fossil Head Formation|41690|5|Briefly described|p5|||||||||
6858|Fossil Head Formation|41731|5|Briefly described|p517|||||||||
6858|Fossil Head Formation|41733|6|Mentioned|Fig.3|||||||||
6858|Fossil Head Formation|41839|6|Mentioned|p33|||||||||
6858|Fossil Head Formation|41864|6|Mentioned|p147|||Probably informal use of name||||||
6858|Fossil Head Formation|42055|4|Described|Fig.1 P52|||||||||
6858|Fossil Head Formation|42442|3|Fully described|p17|Kungurian|Artinskian|Microflora constrains age. Granulatispoities trisinus, Praecolpatites sinuosus, and near the top Mirobaculispora villosa.||||||20-SEP-18
6858|Fossil Head Formation|43661|6|Mentioned|Fig.3|||||||||
6858|Fossil Head Formation|43699|6|Mentioned|Fig.6,p10||Permian|||||||
6858|Fossil Head Formation|43739|6|Mentioned|Fig.5,p38||Early Permian|||||||
6858|Fossil Head Formation|49637|5|Briefly described|Fig. 3|Late Permian|Late Permian|Of the Kinmore Group. Geological Province: Petrel Sub-basin.See also Fig. 6.||||||07-FEB-11
6858|Fossil Head Formation|60386|6|Mentioned|p297, 310||Artinskian|Petrel Sub-basin, Roebuck/Canning Basin. Proximal shelf. ||||||
6858|Fossil Head Formation|60701|5|Briefly described|p12, p13|Permian|Permian|Forms the oil reservoir seal for the Keyling Formation. Geological Province: Bonaparte Basin.||||||10-APR-08
6858|Fossil Head Formation|62837|5|Briefly described|Stratigraphic columns|Early Permian|Early Permian|Of the Kinmore Group.  Age: ~287-~273Ma. Geological Province:  Western Bonaparte Basin, Northern Bonaparte Basin and Petrel Sub-basin (offshore). .||||||01-MAR-10
6858|Fossil Head Formation|64630|5|Briefly described|p31 Fig.2|Kungurian|Artinskian|Province: Bonaparte Basin. Underlies the Pearce Formation, overlies the Kulshill Group and Keyling Formation.  Palynology age: D. byroensis to M. villosa.||||||24-NOV-09
6858|Fossil Head Formation|64690|5|Briefly described|p504 Fig.2 |Kungurian|Early Permian|||||Is overlain by Pearce Formation.||
6858|Fossil Head Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Permian|Bonaparte Basin.||||||
6858|Fossil Head Formation|64694|6|Mentioned|p235 Fig.3, p245 Fig.9|||Acts as seal for Keyling Formation.||||Overlies Keyling Formation. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|67354|5|Briefly described|p72, p73, pp96-97.|Artinskian|Sakmarian|A marine transgression blanketing the region with marine shales.||||Overlies, unconformably to conformably (in the north) the Keyling Formation.|Marine shales.|
6858|Fossil Head Formation|67370|6|Mentioned|p314 Fig.3, p316 Fig.5, p332. |Permian|Permian|||Basal unit in Kinmore Group.||Is overlain by Torrens Formation of Hyland Bay Subgroup.||
6858|Fossil Head Formation|69452|4|Described|p36:8, 11, 15, 18-20|Roadian|Sakmarian|Bhatia et al. (1984). Equivalent to Fossil Head beds of Caye (1968). Petrel Sub-basin, Bonaparte Basin. Marine shelf deposits. Lower part may be prodeltaic. Offshore and onshore. Up to 590m thick.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group) unconformably to conformably (in north). Is overlain unconformably by Pearce Formation (Hyland Bay Subgroup).|Carbonaceous siltstone and mudstone with sandstone and minor limestone. Abundantly fossiliferous.|12-JUL-16
6858|Fossil Head Formation|69454|5|Briefly described|p38:4|Roadian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
6858|Fossil Head Formation|69653|6|Mentioned|p10|Cisuralian|Cisuralian|Petrel Sub-basin.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group). Is overlain by Torrens Formation.||
6858|Fossil Head Formation|69673|5|Briefly described|p153 fig 125, p170 fig 142, p173|Artinskian|Sakmarian|590m thick. Age derived from fossil assemblage.||Kinmore Group||Overlain by Torrens Formation, overlies Keyling Formation|Carbonaceous siltstone and mudstone with sandstone and minor limestone.|
6858|Fossil Head Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3|Roadian|Sakmarian|See also Regional geology: Figs.6-8, p11. Sahul: p2. Vulcan: Fig.2, p2. Regional seal for underlying Keyling Formation. Gas is reservoired in sandstone. Source rock in Sahul Syncline and Vulcan Sub-basin.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group). Is overlain by Torrens Formation (Hyland Bay Subgroup).||12-JUL-16
6858|Fossil Head Formation|70774|5|Briefly described|p5 fig 3|Kungurian|Artinskian|Bonaparte Basin.||||||
6858|Fossil Head Formation|71146|5|Briefly described|p6|Kungurian|Sakmarian|Bonaparte Basin.||||Overlain by the Hyland Bay Subgroup.|Mudstone.|
6858|Fossil Head Formation|71623|6|Mentioned|p346 fig 4, p345 fig 2|Kungurian|Kungurian|Bonaparte Basin. Same as Lower Marine Beds of Dickens et al. (1972)? See also p344.|||||Shale|
6858|Fossil Head Formation|72505|5|Briefly described|p890|Roadian|Artinskian|Southern Bonaparte Basin. Correlated with the Striatopodocarpites fusus zone to the Microbaculispora villosa zone.||||Overlies the Keyling Formation and the Flat Top Limestone. Overlain by the Torrens Formation.||
6858|Fossil Head Formation|73117|6|Mentioned|p15|Kungurian|Sakmarian|Bonaparte Basin, southern.||||Underlain by Keyling Formation (Kulshill Group). Underlain by and equivalent to Flat Top Limestone.||
6882|Frank River Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
6882|Frank River Sandstone|32660|5|Briefly described|Table 6|||||||||
6882|Frank River Sandstone|32728|6|Mentioned|Table 7|||See also Fig.16||||||
6882|Frank River Sandstone|36551|6|Mentioned|Table 12|||||||||
6882|Frank River Sandstone|36888|4|Described|p215|||||||||
6882|Frank River Sandstone|36898|5|Briefly described|Table 1|||||||||
6882|Frank River Sandstone|37462|5|Briefly described|p293|||||||||
6882|Frank River Sandstone|37927|6|Mentioned|p505|||||||||
6882|Frank River Sandstone|38157|6|Mentioned|Table X|||||||||
6882|Frank River Sandstone|39210|5|Briefly described|Fig.18|||||||||
6882|Frank River Sandstone|43855|5|Briefly described|Map Legend||Proterozoic|||||||
6882|Frank River Sandstone|44140|5|Briefly described|p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. 230 m thick.||Duerdin Group||Overlies Fargoo Tillite conformably. Overlain by Moonlight Valley Tillte unconformably.|Dolomitic sandstone; dropped erratics and lenses of boulder conglomerate.|
6882|Frank River Sandstone|44317|4|Described|Table 3||Adelaidean|||||||
6882|Frank River Sandstone|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
6882|Frank River Sandstone|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
6882|Frank River Sandstone|45047|2|Defined|p85|Adelaidean|Adelaidean|Described pp36,40.||||||19-MAY-15
6882|Frank River Sandstone|45112|6|Mentioned|Table 17|||||||||
6882|Frank River Sandstone|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
6882|Frank River Sandstone|63458|6|Mentioned|p873-874, p886-p887, p897 Fig.19. |Cryogenian|Cryogenian|||Unit in Duerdin Group.||Overlies Fargoo Tillite. Is overlain by Moonlight Valley Tillite.|Conglomerate, sandstone.|
6882|Frank River Sandstone|63762|5|Briefly described|p20|||||||||07-FEB-11
6882|Frank River Sandstone|64104|4|Described|p61-80|Neoproterozoic|Neoproterozoic|This paper reinterprets this unit to include part of Ranford Formation in Purnululu area, where it is ~400 m thick. Records continental glaciation.||Duerdin Group||Overlies Fargoo Formation conformably. Is overlain disconformably by Moonlight Valley Formation.|Interbedded sandstone, conglomerate and siltstone.|
6882|Frank River Sandstone|67484|6|Mentioned|p294, p295 Fig.2|Cryogenian|Cryogenian|East Kimberley.||Of the Duerdin Group.||Overlain by Moonlight Valley Tillite. Underlain by Fargoo Tillite.||
6882|Frank River Sandstone|67620|5|Briefly described|p5|Cryogenian|Cryogenian|East Kimberley region.||Duerdin Group.||Overlies Fargoo Formation. Is overlain by Moonlight Valley Formation.||
6882|Frank River Sandstone|68138|6|Mentioned|p153, 156|Neoproterozoic|Neoproterozoic|East Kimberley region.||Duerdin Group.||||
6882|Frank River Sandstone|68244|4|Described|p660,666-668,670|Neoproterozoic|Neoproterozoic|East Kimberly area, Kimberley region.  ~400m thick, marked by a resistant dolomite bed. Sits unconformably on polished indurated sandstone, showing gouges, chatter marks and striations.||Unit of Duerdin Group.||Overlain by Moonlight Valley Formation. Underlain by Fargoo Formation. Correlative to Walsh Fm (Mount House Gp), and Landrigan Fm (Kuniandi Group).|Thickly bedded, massive, graded sandstone; lithic-feldspathic, feldspathic, quartz, silty quartz. Interbedded minor conglomerate, dolomitic sandstone, siltstones. Resistant carbonate cap of karstified interbedded buff laminated dolomicrite.|
6882|Frank River Sandstone|68473|6|Mentioned|p531-532|||||Duerdin Group||Equivalent to the Egan Formation.||
6882|Frank River Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|Includes unnamed mudstone member||Poorly sorted lithic sandstone and dolomitic sandstone, pebble to cobble sandstone, conglomerate, and siltstone; minor thin-bedded dolostone, mudstone and dolomitic mudstone.|31-JUL-15
6882|Frank River Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|||Duerdin Group|||Poorly sorted lithic sandstone and dolomitic, pebble to cobble sandstone, conglomerate and siltstone; minor thin bedded dolostone.|
6882|Frank River Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Duerdin Group.|||Poorly sorted lithic sandstone and dolomitic sandstone, pebble to cobble sandstone, conglomerate, and thin-beddeded mudstone and siltstone; minor thin-bedded dolostone|
6882|Frank River Sandstone|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Poorly sorted lithic sandstone and dolomitic sandstone, pebble to cobble sandstone, conglomerate and siltstone. Minor thin bedded dolostone.|
6882|Frank River Sandstone|71267|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma).|720-635 Ma (inferred)|Unit of Duerdin Group.|||Poorly sorted lithic sandstone and dolomitic sandstone, pebble to cobble sandstone, conglomerate, and siltstone; minor thin-bedded dolostone|
6882|Frank River Sandstone|73255|6|Mentioned|p534 Fig.2, p548 Fig.12|Cryogenian|Cryogenian|||Duerdin Group||Overlies the Fargoo Tillite, underlies the Moonlight Valley Tillite.||
6883|Frank Scott Formation|30388|4|Described|Table 1|||Middle Proterozoic age. Previously Elder Dolomite||||||
6883|Frank Scott Formation|30390|4|Described|p78|||See also P79-80||||||
6883|Frank Scott Formation|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Mission Group||||||
6883|Frank Scott Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
6883|Frank Scott Formation|36551|6|Mentioned|Table 31|||||||||
6883|Frank Scott Formation|36886|4|Described|p198|||||||||
6883|Frank Scott Formation|38988|6|Mentioned|p17|||||||||
6883|Frank Scott Formation|67375|5|Briefly described|p38 Table 1, pp50-51. |Mesoproterozoic|Mesoproterozoic|Siliciclastic and calcareous rocks; sandstones give way to limestones higher in the sequence.||Unit in Mission Group.|Includes Gamminah Conglomerate [?].|Overlies Miller Basalt. Is overlain by Lilian Formation.|Finely-laminated siltstone, dolomitic siltstone, shale, dolomite; minor sandstone and chert; local conglomerate.|12-DEC-16
6883|Frank Scott Formation|67553|4|Described|p40,53-54|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Depositional environment: fluvial (sandstones) to deep marine (shales). ||Unit of Mission Group.|Includes Gamminah Conglomerate.|Overlain by Lilian Formation. Underlain by Gamminah Conglomerate or Miller Basalt.|Fine-grained quartzitic sandstone with abundant altered volcanic detritus, intercalated with fine-grained bluish-green finely laminated siltstones, dolomitic siltstones, shales, and dolomites, as well as minor sandstones and cherts.|
6883|Frank Scott Formation|68995|5|Briefly described|p10, p19, p20|Stenian|Stenian|North of Frank Scott Hill the limestones contain pillow shaped, metre sized, locally domical stromatolites. Lithology discussed in great detail.||Mission Group||Overlies the Miller Basalt and the Gamminah Conglomerate. Overlain by the Lilian Formation.|Finely laminated siltstones, dolomitic siltstones, shales, dolomites, minor sandstones and cherts.|
6883|Frank Scott Formation|69091|5|Briefly described|p75|||||Mission Group|||Sedimentary.|26-SEP-14
6883|Frank Scott Formation|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Mission Group|||Quartzite; basalt and basaltic andesite, epidotized; intercalated limestone, stromatolitic limestone, dolomitic limestone, shale, ripple cross-laminated sandstone; sample descriptions include meta-sedimentary: metasiltstone/metamudstone/metashale|
6883|Frank Scott Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Mission Group.||Overlies Gamminah Conglomerate and Miller Basalt. Is overlain by Lilian Formation. Is intruded by Warakurna Supersuite.|Intercalated limestone, stromatolitic limestone, dolomitic limestone, shale and ripple cross-laminated sandstone.|
6883|Frank Scott Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province|1040 Ma - 1057 Ma (Inferred)|Mission Group|||Intercalated limestone, stromatolitic limestone, dolomitic limestone, shale, and ripple cross-laminated sandstone|
6883|Frank Scott Formation|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Intercalated limestone, stromatolitic limestone, dolomitic limestone, shale, and ripple cross-laminated sandstone|
6883|Frank Scott Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, chert, sandstone, crystalline dolostone/dolomite|
6883|Frank Scott Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1057-1040 Ma (inferred)|Unit of Mission Group.|||Intercalated limestone, stromatolitic limestone, dolomitic limestone, shale, and ripple cross-laminated sandstone|
6884|Frankland Quartz Diorite|40358|4|Described|p10|||||||||
6889|Fraser River Shale|41215|6|Mentioned|p280|||||||||
6902|Frere Formation|7161|5|Briefly described|p90, p99 Fig.9|Orosirian|Orosirian|Earaheedy Basin. Age determined using detrital zircons. Less than 1300m thick.|2027 +/- 23 Ma|||||02-MAY-12
6902|Frere Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Earaheedy Basin.||Of the Tooloo Subgroup.||Overlies Yelma Formation. Is overlain by Windidda Formation.|Granular iron-formation with ferruginous siltstone and chert interbeds.|
6902|Frere Formation|22478|6|Mentioned|p23||Paleoproterozoic|Earaheedy Group, Nabberu Basin||||||07-NOV-08
6902|Frere Formation|22493|6|Mentioned|p90|Orosirian|Orosirian|2027+/-23Ma||||||
6902|Frere Formation|22707|6|Mentioned|P13|||||||||
6902|Frere Formation|23133|5|Briefly described|p293 Fig.1|||Of Earaheedy Basin.||||||19-SEP-06
6902|Frere Formation|23529|4|Described|p13|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup. Max thickness: 1500m. Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23530|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup, Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group, Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23580|5|Briefly described|Map legend||Proterozoic|Of the Earaheedy Group in the Earaheedy Basin.||||||26-AUG-08
6902|Frere Formation|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Earaheedy Group in the Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23587|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23588|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group. Overlain by Windidda Formation. Underlain by Yelma Formation. Earaheedy Basin. Max. thickness: 1300 m.||||||07-NOV-08
6902|Frere Formation|23589|4|Described|p24|||Of Tooloo Subgroup. Overlain by Karri Karri Member. Underlain by Yelma Formation. Earaheedy Basin. Max. thickness: 1200 m.||||||19-SEP-06
6902|Frere Formation|23611|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1.  Of Miningarra Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|23890|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup. Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|24017|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup.  Thickness: 1200m.  Geological Province: Earaheedy Basin.||||||24-MAR-16
6902|Frere Formation|24018|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|24021|5|Briefly described|p16|||Parent: Tooloo Subgroup.  Geological Province: Earaheedy Basin.||||||26-AUG-08
6902|Frere Formation|24578|4|Described|p776 Fig.1, p778 Fig.3|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Overlies the Yelma Formation. Overlain by the Windidda Formation. Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|30010|6|Mentioned|p45|||||||||
6902|Frere Formation|31217|2|Defined|p40|Paleoproterozoic|Paleoproterozoic|Mention p40.||||||07-NOV-08
6902|Frere Formation|31392|4|Described|p3|||Lithology.||||||
6902|Frere Formation|32727|6|Mentioned|p7|||Re Hall & Goode (1975)||||||
6902|Frere Formation|34917|6|Mentioned|p11|||||||||
6902|Frere Formation|35261|6|Mentioned|Table.1|||||||||
6902|Frere Formation|35269|6|Mentioned|p306|||||||||
6902|Frere Formation|35736|6|Mentioned|p24|||||||||
6902|Frere Formation|35975|6|Mentioned|p104|||||||||
6902|Frere Formation|36551|6|Mentioned|Table 29|||||||||
6902|Frere Formation|37021|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|37300|6|Mentioned|p81|||||||||
6902|Frere Formation|37371|6|Mentioned|p363|||||||||
6902|Frere Formation|37460|3|Fully described|p138|||See also p144.||||||19-SEP-06
6902|Frere Formation|38515|4|Described|p10|||||||||
6902|Frere Formation|38516|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|38881|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|38978|3|Fully described|p149|||||||||
6902|Frere Formation|38988|6|Mentioned|p8|||||||||
6902|Frere Formation|39894|5|Briefly described|Fig.2|||||||||
6902|Frere Formation|40089|6|Mentioned|p52|||||||||
6902|Frere Formation|40103|6|Mentioned|Table 1|||||||||
6902|Frere Formation|40354|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|40355|4|Described|p5|||||||||
6902|Frere Formation|40934|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|40938|2|Defined|p19|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
6902|Frere Formation|41997|5|Briefly described|p74|||||||||
6902|Frere Formation|42190|6|Mentioned|p273|||||||||
6902|Frere Formation|42202|6|Mentioned|p512|||||||||
6902|Frere Formation|43069|6|Mentioned|p19|||of Earaheedy Group||||||
6902|Frere Formation|43595|5|Briefly described|p344,Fig.3-42,p345|||||||||
6902|Frere Formation|43652|5|Briefly described|p381|||||||||
6902|Frere Formation|44142|5|Briefly described|p321|||Clasts of the peloidal iron-formation are a distinctive element in Scorpion Subgroup.||Earaheedy Group|||Includes peloidal iron-formation.|
6902|Frere Formation|50188|5|Briefly described|p2 Fig. 1, p3,|||Of the Tooloo Subgroup (Earaheedy Group). Conformably underlies Karri Karri Formation.  Max. thickness: ~1200m.  Geological Province: Earaheedy Basin.||||||16-JUL-08
6902|Frere Formation|50195|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup, Earaheedy Group. Includes the Windidda Member.  Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|50216|6|Mentioned|p213|||Geological Province: Earaheedy Basin.||||||
6902|Frere Formation|50222|3|Fully described|p320 Fig. 3, p328|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Consists of four major granular iron-formation intervals, separated by at least 3 major shale and siltstone bands, and minor carbonate. Max. thickness: ~600m. Geological Province: Earaheedy Basin. See also p317.||||||07-NOV-08
6902|Frere Formation|50223|5|Briefly described|p345 Fig. 2, p346|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group).  Consists of four granular iron-formation intervals interbedded with at least three shale dominated bands.  Max. thickness: ~600m.  Geological Province: Earaheedy Basin.||||||01-MAR-10
6902|Frere Formation|50224|5|Briefly described|p368, p370|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Peloidal, shaly and banded iron-formation; chert, shale, minor carbonate. Max. thickness: ~600m. Geological Province: Earaheedy Basin.||||||07-FEB-11
6902|Frere Formation|50226|5|Briefly described|p423, p424|||Middle part of the Tooloo Subgroup (Earaheedy Group).  Granular iron-formation and shale. Overlies Yelam Formation; underlies Wididda Formation. Geological Province: Earaheedy Basin.  See also p426.||||||26-AUG-08
6902|Frere Formation|50309|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Earaheedy Basin. Of the Tooloo Subgroup (Earaheedy Group). Overlies: Yelma Formation.  Underlies: Karri Karri Member, Windidda Formation.||||||07-NOV-08
6902|Frere Formation|50319|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Granular and laminar iron-formation, granular silicious iron-formation, siltstone, shale, and chert; marine deposits.||||||07-NOV-08
6902|Frere Formation|50334|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin||||||07-NOV-08
6902|Frere Formation|50378|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Overlain by Windidda Formation. Overlies Yelma Formation. Geological Province: Earaheedy Basin. Lithology: granular iron-formation, granular siliceous iron-formation, siltstone, shale jasper, and chert.||||||07-NOV-08
6902|Frere Formation|50626|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Earaheedy Group.  Geological Province: Earaheedy Basin.||||||07-NOV-08
6902|Frere Formation|61564|5|Briefly described|p589, p591|||Of the Earaheedy Group. Includes granular iron formation exhibiting cross-cutting quartz veining, partially silicified; siltstone and shale, minor iron formation and chert. ||||||
6902|Frere Formation|61732|5|Briefly described|p26|Mesoproterozoic|Mesoproterozoic|Of the Earaheedy Group. Contains assemblages of microfossils.||||||07-FEB-11
6902|Frere Formation|63866|5|Briefly described|p166|||Eraheedy Basin.||Tooloo Subgroup||Overlies the Yelma Formation. Overlain by the Windidda Formation.||
6902|Frere Formation|64284|4|Described|p58 Fig. 1, p59|Paleoproterozoic|Paleoproterozoic|Of the Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Consists of 3 major granular iron-formation intervals, separated by up to 3 major shale/siltstone bands, + minor carbonate.Detailed lithology given.||||||07-FEB-11
6902|Frere Formation|64285|5|Briefly described|p65, p66-67 Figs.1,2|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Granulare iron-formation interbedded with shale.||||||07-FEB-11
6902|Frere Formation|64580|4|Described|map legend||Paleoproterozoic|Of Tooloo Subgroup. Peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, and sandstone.||||||09-DEC-08
6902|Frere Formation|64655|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tooloo Subgroup (Earaheedy Group). Geological Province: Earaheedy Basin. Granular iron-formation and granular silliceous iron-formation, in places peloidal; minor siltstone, shale, and chert.||||||
6902|Frere Formation|64725|6|Mentioned|p59.|||BIF beds constitute a significant iron resource.||Middle unit in Tooloo Subgroup.||Overlies Yelma Formation; underlies Windidda Formation.||24-SEP-14
6902|Frere Formation|64748|6|Mentioned|p276, Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
6902|Frere Formation|64772|4|Described|p9, Plate 1,  p10 Fig. 5|Paleoproterozoic|Paleoproterozoic|Stanley Fold Belt. Economic potential for iron; prospective for manganese mineralisation. Thickness: 1200 m (of Bunting, 1986, may include structural repetition); ~600m (Hocking and Jones (2002).Eight distinct microbial assemblages (Tobin 1990) deposited on shoals above storm wavebase. The granular iron-formation has strong magnetic signature through significant overburden. Geol.prov: Earaheedy Basin. See also p8 Fig.4, p11, p17, p19 Fig.9, p20-21 (incl. Fig.10), p25 Fig.11, p25 Fig.12, p26 Fig.13, p27 Fig.15, p28 Fig.16, p29 Fig.17, p32 Fig.20, p33 Fig.21, p36-37, p38 Tb.9, p39-43, p44 Fig.30, p45, p46, p50-51, p69 App.4, p70-71 App.4 Tb.4.2, p72-74 Fig.4.1, p75 Tb.4.3, p76-77 Fig.4.2, p78 App.4 Tb.4.4, p79-81 App.4 Fig.4.3.||Of Tooloo Subgroup (Earaheedy Group)|Includes Windidda Member, Canning Gap Shale Member|Conformably overlies Yelma Formation|Typically consists of granular and supergene-enriched iron-formation (resistant strike ridges and cuestas) separated by more abundant shale (in valleys or broad, colluvium -covered flats), siltstone, chert, and jasper beds.|25-NOV-13
6902|Frere Formation|65264|5|Briefly described|p27, p32, p44 Appdx. 1|Paleoproterozoic|Paleoproterozoic|Basal unit of the Tooloo Subgroup (Earaheedy Group). Conformably overlies Yelma Formation. Geological province: Earaheedy Basin. Has up to 3 units of granular iron-formation (further details included).||||||07-FEB-11
6902|Frere Formation|65419|5|Briefly described|p46, p47.|Paleoproterozoic|Paleoproterozoic|Age from stromatolitic carbonates.|1946 +/- 71 Ma (Pb-Pb age; Russell et al. 1994).|Unit in Earaheedy Group.||Conformably overlies the Yelma Formation.||
6902|Frere Formation|65472|5|Briefly described|p1, p3 Fig.2, p5 Fig.4, p6, p8 Fig.6|||Thickness: ~600 m. Earaheedy Basin.||Tooloo Subgroup||Overlies Yelma Formation, including Sweetwaters Well Member; is overlain by Windidda Member.|Lake Superior-type granular iron-formation and shale; minor ash-tuff beds.|
6902|Frere Formation|65692|5|Briefly described|p9-10, p12, p55-56|||Formed in a shallow marine environment; cyclic changes in sea level produced cyclic sediment patterns. c.600m thick.||Tooloo Subgroup.|Includes Windidda Member.|Overlies Yelma Formation. Is overlain by Chiall Formation.|Consists of four intervals of granular iron beds separated by shales, siltstones and carbonates; includes BIF, siltstone, shale, massive green chert, and granular iron-formation.|06-MAR-17
6902|Frere Formation|65899|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Unit in Earaheedy Group. Peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, sandstone.||||||
6902|Frere Formation|65913|5|Briefly described|p4. ||||1946 +/- 71 Ma (Russell et al. 1994).||||Includes stromatolitic carbonates.|
6902|Frere Formation|66115|6|Mentioned|p146|||Duck Creek Dolomite is compared with micropaleontology from other sites around the world, and Frere Formation in Australia.||||||
6902|Frere Formation|66427|5|Briefly described|p39-43, p46 Fig.4, p47-63, p70-74|||Of Hall et al. (1977). Redefined here to include the former Windidda Formation as Windidda Member. Contains Gunflint-type microbial assemblages. Records the onset of major Fe-oxide precipitation; contains economic iron deposits.||Of the Tooloo Subgroup.|Includes Windidda Member.|Overlies Sweetwaters Well Member (Yelma Formation). Is overlain conformably (transitionally) by Karri Karri Member (Chiall Formation).|Granular iron-formation. Total thickness ~600m. Consists of alternating beds of haematitic shale, green chloritic siltstone and granular iron-formation; has minor carbonate and thin volcaniclastic horizons.|
6902|Frere Formation|67827|6|Mentioned|p421 Fig.10|||Said to be of the Nabberu and Earaheedy Basins. Contains material described as platy hematite and specularite, and as microplaty hematite; authors prefer 'dehydrated goethite pseudomorphs after silicate'.|||||Granular iron formation.|
6902|Frere Formation|67855|5|Briefly described|p208 fig 3-8, p209|Paleoproterozoic|Paleoproterozoic|||Tooloo Subgroup|||Iron formation, shale, chert.|
6902|Frere Formation|68055|5|Briefly described|p77-78, 87|Proterozoic|Proterozoic|Earaheedy Basin. Basal boundary is the first major occurrence of chert or granular iron formation. Contains microbial microfossils.||Tooloo Subgroup.|Windidda Member.|Gradationally overlies Yelma Formation.|Granular iron formation interlayered with carbonate, siltstone and shale beds.|
6902|Frere Formation|68141|5|Briefly described|p190, 192, 196|Paleoproterozoic|Paleoproterozoic|Stable Si isotope data tabulated; remarkably low delta30Si discussed.|1800 Ma.|||Possibly coeval with Duck Creek Formation.|Oolitic iron formation.|
6902|Frere Formation|68471|6|Mentioned|p19 Tb.3, p20|||U-Pb dating on interbedded volcanic ash units by Rasmussen et al. (2012).|c.1890 Ma.|||||
6902|Frere Formation|69003|4|Described|p13 Fig.17, p14-15|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin. c.600m thick. Age from magmatic zircons from tuffaceous layers.|c.1890 Ma (SHRIMP U-Pb).|Tooloo Group.|Windidda Member.|Overlies Yelma Formation. Is overlain unconformably by Chiall Formation (Miningarra Group).|Granular iron formation, shale and siltstone, stromatolitic carbonate rock.|
6902|Frere Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin||Tooloo Subgroup|Includes Windidda Member.||Peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, and sandstone.|06-AUG-15
6902|Frere Formation|69153|6|Mentioned|Rocks.csv||||||||Sample descriptions include: chert (laminated, dark, dense, plus quartz veining) and iron formation (BIF and chert; black aphanitic; strongly magnetic)|
6902|Frere Formation|69313|4|Described|vii, p2-3, p6, p12-13, p16-p19, p21-p54|Paleoproterozoic|Paleoproterozoic|Thickness c.600m (originally estimated at 1200-1300m). Deposited in shallow marine, middle shelf or arid coastline environments during a marine transgressive cycle. Stromatolites are present. Age based on stratigraphic relationship with the underlying 1.81 Ga Yelma Formation. Lithology and lithofacies illustrated and discussed in great detail from p26-p50. Paragenesis and diagenesis discussed in great detail. See also p57-58, p60-61, p63-65, p87-p90, p92-p94, p96-p103, p115.|c. 1800 Ma.|Tooloo Subgroup|Windidda Member.|Unconformably (or disconformably) overlies the Yelma Formation. Overlain unconformably by the Chiall Formation (Minningarra Subgroup).|Iron formation, siltstone and hummocky cross-stratified sandstone that grades into microbially laminated, hematite-rich mudstone.|21-JAN-22
6902|Frere Formation|69596|5|Briefly described|p10|||Earaheedy Basin.||Tooloo Group.|Windidda Member.|||
6902|Frere Formation|70153|5|Briefly described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_geologyp14_lut.csv and 500k_interpgeop14_lut.csv.|2027 +/- 23 Ma (isotopic) - 1600 Ma (inferred).|Tooloo Group|Windidda Member||Peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, and sandstone.|
6902|Frere Formation|70804|5|Briefly described|p20|||Earaheedy Basin. ||||Correlated with the Robinson Range Formation.|Includes granular iron-formation.|27-FEB-23
6902|Frere Formation|71169|6|Mentioned|p82|Orosirian|Orosirian|West Australian Craton. |c. 1880 Ma (Rasmussen et al., 2012)|||||
6902|Frere Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||iron formation, siltstone, sandstone, chert|
6902|Frere Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy Basin. Events: Edmundian Orogeny (1026 - 954 Ma); Mangaroon Orogeny (1682 - 1619 Ma); Stanley Fold Belt deformation (2005 - 1620 Ma); Mangaroon Orogeny D2m/M2m (1677 - 1659 Ma); Mangaroon Orogeny D1m/M1m (1682 - 1677 Ma).  See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 100k_geologyp14_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop_lut.csv.|2027+\-23 Ma; 1650 Ma inferred|Unit of Tooloo Subgroup.|Incldues Windidda Member.||Undivided; peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, and sandstone|
6902|Frere Formation|71484|4|Described|p121,123-125,130-132,137-139|Orosirian|Orosirian|Geological province: Earaheedy Basin. Thickness: 600-1200m. Deposited in a shallow-marine setting. Contains thin tuff layers dated at c. 1890 Ma (Rasmussen et al., 2012), indicating a 60my hiatus with the underlying Yelma Formation. Possibly age equivalent to the Robinson Range Formation, deposited in a large extensional basin, deepening to the W and N.|<1890 Ma|Unit of Tooloo Group.|Includes Windidda Member.|Overlain unconformably by Chiall Formation/Miningarra Group. Underlain unconformably by Imbin Porphyry.|Granular ironformation, jasperoidal chert, granular siliceous-formation, iron-rich siltstone and mudstone, and sandstone, with minor tuffaceous lenses.|30-AUG-19
6902|Frere Formation|71798|4|Described|p109-p113, p115, p117|Orosirian|Orosirian|Earaheedy Basin. Up to 600m thick. The monazite dated tuff layer is intersected in diamond drillhole TDH26 at 386.4m depth and is interbedded with the granular iron formation.|1891 +/- 9 Ma (Monazite U-Pb)|Tooloo Group|||Granular Iron formation and fine-grained, clastic sedimentary rocks.|
6902|Frere Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin.|Max age 2027+/-23 Ma, min ~1650 Ma.|Tooloo Group|||Peloidal chert, granular iron-formation, granular siliceous iron-formation, siltstone, and sandstone.|
6911|Frezier Sandstone|7433|5|Briefly described|p25 Fig.2,  p42, pp45-47. |Aptian|Aptian|Canning Basin. Fluvial clastics. 30 m thick. Disconformably underlies Anketell Sandstone.||||Disconformably overlies Broome and Melligo Sandstones, and Parda Formation. Probably overlies Jarlemai Siltstone and Alexander Formation; also Callawa Formation where Parda Formation is missing.|Sandstone, locally feldspathic; ferruginised by weathering.|
6911|Frezier Sandstone|22717|6|Mentioned|p20|||||||||10-FEB-20
6911|Frezier Sandstone|22718|6|Mentioned|p8||Aptian|||||||10-FEB-20
6911|Frezier Sandstone|22738|4|Described|9,14,17, map|Early Cretaceous|Early Cretaceous|Max thickness 20 m. Underlying units Parda Formation, Broome Sandstone||||||
6911|Frezier Sandstone|22765|5|Briefly described|p11, Table1||Aptian|Possibly equivalent to the Parda Formation||||||10-FEB-20
6911|Frezier Sandstone|22801|5|Briefly described|p13, Table1 p8||Early Cretaceous|Equivalent to Callawa Formation||||||10-FEB-20
6911|Frezier Sandstone|23212|4|Described|Table.1 p11||Aptian|Rare bivalves outside the sheet area.||||||
6911|Frezier Sandstone|23575|5|Briefly described|Map Legend|Mesozoic|Mesozoic|||||||
6911|Frezier Sandstone|32648|6|Mentioned|p32|||Lower Cretaceous.||||||
6911|Frezier Sandstone|34363|6|Mentioned|p56|||Aptian. See Fig.7||||||
6911|Frezier Sandstone|36257|6|Mentioned|Table 2.1|||||||||
6911|Frezier Sandstone|36438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|36632|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|36890|3|Fully described|p352|||||||||
6911|Frezier Sandstone|37368|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|37369|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|37370|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|38878|6|Mentioned|Map legend|Aptian|Neocomian|Neocomian - Aptian||||||
6911|Frezier Sandstone|39857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|40078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|43563|6|Mentioned|Fig2,p5||Early Cretaceous|||||||
6911|Frezier Sandstone|43656|6|Mentioned|Fig.2,p8|Aptian|Barremian|||||||
6911|Frezier Sandstone|43746|6|Mentioned|Fig.2,p11|Aptian|Barremian|||||||
6911|Frezier Sandstone|44143|4|Described|p431 Table 4-19|Cretaceous|Cretaceous|Up to 20m thick; fine to coarse sandstone; minor granule conglomerate; fluvial to deltaic. Disconformably overlies Parda Formation, and Melligo and Broome Sandstones; is overlain disconformably by Anketell Sandstone. Type section at Cape Frezier (LAGRANGE: 18deg 52' 00" S, 121deg 36' 20" E).||||||10-FEB-20
6911|Frezier Sandstone|44357|4|Described|p14,Tb.1 p8||Early Cretaceous|||||||
6911|Frezier Sandstone|44443|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|||||||
6911|Frezier Sandstone|44479|2|Defined|Tb.1|||E/51-1. Correlates with Anketell Sandstone of this Sheet.||||||13-DEC-22
6911|Frezier Sandstone|44998|2|Defined|p183||Aptian|Overlies Anketell-Parda Formation. On many pages. p.133,155,157,162,188,199,map. See also App.4 p283.||||||
6911|Frezier Sandstone|45153|2|Defined|App.8-134|Aptian|Aptian|Type section: Cape Frezier (18degrees57'S, 121degrees33'E). Li tbology: At the type area the unit consists of cross-bedded sandstone, conglomeratic sandstone, and minor siltstone. In Goldwyer No. 1 it  occurs as a sandstone: very fine to very coarse-grained, poorly sorted, slightly micaceous angular with occasional conglomerate beds.||||||13-DEC-22
6911|Frezier Sandstone|45158|3|Fully described|p12|||||||||
6911|Frezier Sandstone|46319|4|Described|p18|Early Cretaceous|Early Cretaceous|Geological Province: Canning Basin.||||||
6911|Frezier Sandstone|50544|4|Described|p65, p16 Tb. 1|Cretaceous|Cretaceous|Fluvial deltaic deposits of ferruginised, partly bioturbated, poorly sorted, coarse-grained sandstone, conglomerate, and minor siltstone.  Disconformably overlies the Parda Formation.  Age: 120.5-98.9Ma.  Geological Province:  Canning Basin.  See also p62.||||||13-DEC-22
6911|Frezier Sandstone|50555|5|Briefly described|Map legend|Cretaceous|Cretaceous|Poorly sorted, coarse-grained, partly bioturbated sandstone, conglomerate, and minor siltstone.  Geological Province: Canning and Northern Cararvon Basins (Westralian Superbasin).||||||23-DEC-09
6911|Frezier Sandstone|64449|5|Briefly described|p62 Tb. 2|Early Cretaceous|Early Cretaceous|Consists of poorly bedded, fine to coarse, poorly sorted sandstone and minor conglomerate.||||||07-FEB-11
6911|Frezier Sandstone|64580|4|Described|map legend||Early Cretaceous|Fine- to coarse-grained sandstone; minor conglomerate.||||||09-DEC-08
6911|Frezier Sandstone|64643|5|Briefly described|p3 Fig. 2|Early Cretaceous|Early Cretaceous|||||||10-FEB-20
6911|Frezier Sandstone|65301|5|Briefly described|p5 Fig. 4|Early Cretaceous|Early Cretaceous|Geological province: Canning Basin.||||||
6911|Frezier Sandstone|65449|6|Mentioned|p6|Early Cretaceous|Early Cretaceous|||||Overlies Broome Sandstone. Is overlain by Bejah Claystone.||
6911|Frezier Sandstone|67202|5|Briefly described|p44 Fig.2.10, p69-71, p126, p128|Early Cretaceous|Early Cretaceous|See also p135-136, p277. Canning Basin. Thickness of 15m exposed. Fluvial to deltaic deposits. Thought to be a basinward facies of Callawa Formation. Conductivity images.||||Overlies Callawa and Parda Formations. Is overlain disconformably by Anketell Sandstone.|Sandstone, fine- to coarse-grained, minor conglomerate, poorly sorted, feldspathic in part; commonly ferruginised or pedogenically altered.|
6911|Frezier Sandstone|68007|6|Mentioned|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||||25-FEB-20
6911|Frezier Sandstone|68902|6|Mentioned|p9 fig 5|Cretaceous|Cretaceous|||||Overlies Broome Sandstone, overlain by Bejah Claystone.||
6911|Frezier Sandstone|69182|6|Mentioned|Ch4 p9, Ch4 p45, Ch4 p47|Cretaceous|Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Bejah Claystone and the Anketell Formation.||
6911|Frezier Sandstone|69297|6|Mentioned|p337, p352|Aptian|Aptian|Broome Platform of the Canning Basin. ||||Overlies the Parda Formation.||
6911|Frezier Sandstone|69590|4|Described|250k_interpgeop_lut.csv|Early Cretaceous|Early Cretaceous|Of Canning Basin.|145-101 Ma (inferred)||||Fine- to coarse-grained sandstone; minor granule conglomerate.|13-DEC-22
6911|Frezier Sandstone|70774|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Bejah Claystone.||10-FEB-20
6911|Frezier Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
6911|Frezier Sandstone|71894|5|Briefly described|p4|Early Cretaceous|Early Cretaceous|Canning Basin.||||Overlies the Broome Sandstone. Overlain by the Bejah Claystone and the Anketell Formation.|Sandstone.|10-FEB-20
6911|Frezier Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Early Cretaceous|Early Cretaceous|Canning Basin.  Age from biostratigraphy.|||||Fine- to coarse-grained sandstone; minor granule conglomerate.|
6911|Frezier Sandstone|72499|5|Briefly described|p7 Fig.6.|Early Cretaceous|Early Cretaceous|Located in the Broome Platform.||||Overlies Broome Sandstone. Underlies Bejah Claystone and Anketell Formation. Laterally equivalent to Samuel and Parda Formations.||
6911|Frezier Sandstone|73117|5|Briefly described|p3|Lower Cretaceous|Lower Cretaceous|Canning Basin.||||Underlain by Broome Sandstone. Overlain by Bejah Claystone and Anketell Formation. Equivalent to Samuel Formation, Parda Formation, and Melligo Sandstone.|Dominantly sandstone.|
6911|Frezier Sandstone|73574|5|Briefly described|p761-763|Aptian|Aptian|Northern and western Pilbara Craton. Fluviodeltaic.||||Overlies Callawa Formation in places|Ferruginised, partly bioturbated, poorly sorted, coarse-grained sandstone, conglomerate and minor siltstone.|
6954|Gage Sandstone|12758|1|Redefined|p21, p3 Fig. 3|Neocomian|Neocomian|Supersedes Gage Sandstone Member (Bozanic, 1969a) and Gage Formation Davidson (1995). Of the Warnbro Group. Type section redefined to interval between 1587 and 1704  m in Gage Roads 1, on palynolological evidence. Overlain conformably by the South Perth Shale; unconformably overlies the Parmelia Group.  Max. thickness: 259m. Geological Province: Perth Basin.||||||04-SEP-14
6954|Gage Sandstone|14227|5|Briefly described|p12, Enclos. 2|Barremian|Valanginian|Of the Warnbro Group. Geological Province: Vlaming Sub-basin. Submarine sediments, including turbidites.||||||07-FEB-11
6954|Gage Sandstone|24443|5|Briefly described|Fig.31|Early Cretaceous|Early Cretaceous|Of Warnbro Group. Overlies Bunbury Basalt (unconformable). Overlain by South Perth Shale. Geological Province: Perth Basin.||||||
6954|Gage Sandstone|30217|6|Mentioned|p20|||Correlation P20. Hydrogeology P24||||||
6954|Gage Sandstone|60376|5|Briefly described|p17 Fig. 4.|Early Cretaceous|Early Cretaceous|Geological Province: Perth Basin. Of the Warnbro Group. Overlain by South Perth Shale. Underlain unconformably by Charlotte Sandstone (Parmelia Group).||||||07-FEB-11
6954|Gage Sandstone|67925|5|Briefly described|Ch2 p10 fig 4|Valanginian|Berriasian|||||Unconformably overlies the Parmelia Group. Overlain by the South Perth Shale.||
6954|Gage Sandstone|69081|5|Briefly described|p737 Fig.1|Early Cretaceous|Early Cretaceous|Presented as Gage Sst in figure. Geol. Prov: Perth Basin||Warnbro Group||Is overlain by South Perth Shale; unconformably overlies Parmelia Group.||23-JUL-15
6954|Gage Sandstone|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p55, Ch2 p57|Lower Cretaceous|Lower Cretaceous|Perth Basin. ||Warnbro Group||Unconformably overlies the Parmelia Group. Overlain by the South Perth Shale.||
6954|Gage Sandstone|69297|6|Mentioned|p174, p175, p189|Valanginian|Berriasian|Vlaming Sub-basin. Deposited in a marine or deltaic environment. ||Warnbro Group||Overlies the Bunbury Basalt. Overlain by the South Perth Shale.||
6954|Gage Sandstone|70097|5|Briefly described|p19 Fig.3|Valanginian|Valanginian|Southern Perth Basin. Vlaming Sub-basin.||Warnbro Group||Overlies Charlotte Sandstone (Parmelia Group). Is overlain by South Perth Shale.||12-SEP-17
6954|Gage Sandstone|70099|5|Briefly described|Fig.4; p5|Valanginian|Valanginian|Vlaming Sub-basin. Correlated to the Mentelle 5 syn-breakup Supersequence. Marine to deltaic.||Warnbro Group.||Overlies Bunbury Basalt. Is overlain by South Perth Shale.||
6954|Gage Sandstone|70128|5|Briefly described|p449, p451, p456, p458-463|Early Cretaceous|Early Cretaceous|Central Perth Basin. 610m thick. Modelled thickness distribution histogram.||Warnbro Group.||Unconformably overlies Parmelia Group. Is overlain conformably by South Perth Shale.||
6954|Gage Sandstone|71958|4|Described|p2, p6-p9, p11, p16, p18, p20, p36, p41|Early Cretaceous|Early Cretaceous|Vlaming Sub-basin, Perth Basin. The Gage Sandstone Member was initially introduced by West Australian Petroleum Pty Ltd (1969) and formally recognised by Playford et al. (1976) as a member of the South Perth Shale. Davidson (1995) elevated the unit to the Gage Formation which has been superseded. Crostalla and Backhouse 2000 outlined the unit.This unit is laterally extensive (over 1500km2) and reasonably thick (100-300m). Forms a potential CO2 storage reservoir that overlies syn-rift reservoir units. Storage capacity of the reservoir is measured at 126 million tonnes at P50 and 493 million tonnes at P50 and 1360 million tonnes at P10. Intersected in eight wells; however, conventional core was only recovered from Gage Roads 1 and Warnbro 1. Identified by Gagiella mutabillis marine dinoflagellate zone. Good potential for CO2 storage. See also p54, p56, p98, p109, p115, p118, p136-p138, p140, 162.||Warnbro Group||Unconformably overlies the Charlotte Sandstone. Overlain by the South Perth Shale.|Sandstones.|
6954|Gage Sandstone|72258|5|Briefly described|p129|Early Cretaceous|Early Cretaceous|Of Perth Basin.||||Overlain by South Perth Shale. Underlain unconformably by Parmelia Group.||
6959|Galah Monzogranite|24196|5|Briefly described|p44|Archean|Archean|Age: 2647 +/- 7 Ma (Dunphy et al., in prep)||||||07-NOV-08
6959|Galah Monzogranite|24494|5|Briefly described|p21, p38 App.1|||See also Galah monzogranite.||||||
6959|Galah Monzogranite|42626|6|Mentioned|Fig.14 P39|||Reserved as Galah Monzonite.||||||
6959|Galah Monzogranite|42904|5|Briefly described|map legend|||||||||
6959|Galah Monzogranite|43215|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
6959|Galah Monzogranite|43234|6|Mentioned|p5|||||||||
6959|Galah Monzogranite|43478|2|Defined|p4-44|||||||||
6959|Galah Monzogranite|50075|5|Briefly described|p17|Archean|Archean|Geological Province: Yilgarn Craton.||||||23-DEC-09
6959|Galah Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite monzogranite.  Geological Province: Yilgarn Craton.||||||23-DEC-09
6959|Galah Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Muscovite-biotite monzogranite; numerous pegmatite segregations.||||||07-FEB-11
6959|Galah Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Muscovite-biotite monzogranite; numerous pegmatitic segregations.|06-AUG-15
6959|Galah Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2642 +/- 8 Ma (isotopic).||||Muscovite-biotite monzogranite; numerous pegmatitic segregations.|
6959|Galah Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
6959|Galah Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|2642+\-8 Ma ||||Muscovite-biotite monzogranite with numerous pegmatitic segregations; metamorphosed|
6969|Gallup Sandstone|39316|6|Mentioned|p327|||||||||
7009|Gardiner Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group.  Age: <1790Ma (Smith 2001).  Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|22446|5|Briefly described|p20|Calymmian|Calymmian|||||||
7009|Gardiner Sandstone|22496|3|Fully described|p9||Mesoproterozoic|Age: 1560 +/- 20 Ma.  Of the Birrindudu Group. Unconformably overlies the Archaean Browns Range Metamorphics. Overlain unconformably by Lewis Range Sandstone. Max. thickness: >1000m. Geological Province: Birrindudu Basin.||||||22-DEC-08
7009|Gardiner Sandstone|22716|6|Mentioned|p237|Mesoproterozoic|Mesoproterozoic|||||||
7009|Gardiner Sandstone|22764|6|Mentioned|p5|||BILLILUNA Sheet area. Birrindudu Basin.||||||01-FEB-10
7009|Gardiner Sandstone|22777|5|Briefly described|Map|||Birrindudu Group, Birrindudu Basin.||||||22-DEC-08
7009|Gardiner Sandstone|23117|5|Briefly described|p445|||||||||
7009|Gardiner Sandstone|23314|6|Mentioned|332|||||||||
7009|Gardiner Sandstone|23621|3|Fully described|p31|Mesoproterozoic|Mesoproterozoic|Age: 1560+/-20 Ma (K-Ar). See also page 10 Table 1. Of Birrindudu Group. Underlying unit Browns Range Metamorphics (unconformably). Geological Province: Birrindudu Basin.||||||19-SEP-06
7009|Gardiner Sandstone|23622|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Group. Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|23809|5|Briefly described|p9|||Of the Birrindudu Group.  Overlies unconformably Pargee Sandstone.||||||19-SEP-06
7009|Gardiner Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Birrindudu Group. Overlies Inverway Metamorphics; overlain by Talbot Well Formation. Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Birrindudu Group.  Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|29804|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7009|Gardiner Sandstone|29805|4|Described|Table 1|||||||||
7009|Gardiner Sandstone|29809|5|Briefly described|p418|||||||||
7009|Gardiner Sandstone|29811|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
7009|Gardiner Sandstone|29812|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7009|Gardiner Sandstone|29813|4|Described|Table 2|||||||||
7009|Gardiner Sandstone|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7009|Gardiner Sandstone|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
7009|Gardiner Sandstone|31361|4|Described|Table 1|||See also age dates Table 2.||||||
7009|Gardiner Sandstone|31362|4|Described|Table 1|||||||||
7009|Gardiner Sandstone|32728|6|Mentioned|p38|||||||||
7009|Gardiner Sandstone|35205|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7009|Gardiner Sandstone|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
7009|Gardiner Sandstone|36551|6|Mentioned|Table 12|||||||||
7009|Gardiner Sandstone|36902|6|Mentioned|p12|||||||||
7009|Gardiner Sandstone|37299|6|Mentioned|Fig.1|||||||||
7009|Gardiner Sandstone|37371|6|Mentioned|p368|||||||||
7009|Gardiner Sandstone|37577|6|Mentioned|p49|||||||||
7009|Gardiner Sandstone|38482|6|Mentioned|Table 2|||||||||
7009|Gardiner Sandstone|41125|6|Mentioned|p30|||||||||
7009|Gardiner Sandstone|42504|5|Briefly described|Table 3 P60|||||||||
7009|Gardiner Sandstone|43300|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7009|Gardiner Sandstone|43301|5|Briefly described|Map Legend||Mesoproterozoic|Of Birrindudu Group.||||||19-SEP-06
7009|Gardiner Sandstone|43303|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7009|Gardiner Sandstone|44155|6|Mentioned|p252|Mesoproterozoic|Mesoproterozoic|K-Ar and Rb-Sr age from glauconite.|c.1.56 Ga (Blake et al., 1979).|||Correlated with Mount Parker Sandstone.||
7009|Gardiner Sandstone|45140|2|Defined|p2, p13, p16, p18, p20-25, p32, p39-43|||See also p47, p53-56, p58, p67, p69, p74, p76-77, p80-83, Appx.p16-17. Originally the Gardiner Beds of Casey and Wells (1966); see references to that unit (p39, p43-44, p48, p50). A mis-spelling: named after the Gardner [sic] Range (Davidson, 1905), incorrectly spelt Gardiner on most WA maps. Raised to Formation rank by Blake et al. (1975). Birrindudu Basin. 3000m thick. Forms prominent ridges and hills. The type section is at Larranganni Bluff, at the S end of Gardner Range; that sequence and three others are detailed. Local silcrete. Basal 6m contains anomalous uranium. Source of potable borewater at Tanami. Is overlain by Larranganni Beds, Talbot Well Formation conformably and Lewis Range Sandstone unconformably. Is faulted against and ?unconformably overlies Winnecke Granophyre. May correlate with Mount Parker Sandstone and Limbunya Group. Appears as Gardiner Formation on p74. Age from glauconitic sandstone.|1560+/- 20 Ma (K-Ar age).|Basal Birrindudu Group.||Unconformably overlies Killi Killi, Mount Charles, Nongra and Nanny Goat Creek Beds (Tanami Complex), Pargee and Supplejack Downs Sandstones, Mount Winnecke Formation, Lewis Granite.|Sublithic arenite and subordinate quartz arenite, mostly medium-grained, variably iron-stained; conglomerate, common at/near the base; interbedded shale, siltstone and fine-grained arenite; glauconitic sandstone; local dolomitic sandstone.|
7009|Gardiner Sandstone|46788|4|Described|p10|||||||||
7009|Gardiner Sandstone|46864|4|Described|p37|||||||||
7009|Gardiner Sandstone|48950|2|Defined|p33|Neoproterozoic|Neoproterozoic|||||||
7009|Gardiner Sandstone|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group.  Includes the Glauconitic Sandstone member (informal). Sandstone - white, sublithic arenite, quartz arenite, conglomerate, siltstone and shale; thin to thick bedded, medium- to coarse-grained, poorly sorted.||||||07-NOV-08
7009|Gardiner Sandstone|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Includes Glauconitic Sandstone member (informal)||||||07-NOV-08
7009|Gardiner Sandstone|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Includes the informal Glauconitic Sandstone member. Sandstone - white sublithic arenite, quartz arenite, conglomerate, siltstone and shale, thin to thick bedded, medium- to coarse-grained, poorly sorted.||||||07-NOV-08
7009|Gardiner Sandstone|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Includes Glauconitic Sandstone member. Sandstone: white, sublithic arenite, quartz arenite, conglomerate, siltstone and shale; thin to thick bedded, medium to coarse grained, poorly sorted.||||||07-NOV-08
7009|Gardiner Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Birrindudu Group. Geological Province: Birrindudu Basin.||||||
7009|Gardiner Sandstone|61861|4|Described|p9, p16, p20, pp22-24, Figs.35-37.|Statherian|Statherian|Ware Range. Forms prominent ridges. 1000 m thick. K-Ar and Rb-Sr dating of glauconite (1560 Ma) is considered unreliable and a gross underestimate of the age (Blake et al. 1979).||Basal unit in Birrindudu Group.||Overlies Nanny Goat Volcanics. Interpreted to overlie MacFarlane Peak Group near Supplejack Station.|Basal conglomerate; medium- to thick-bedded, sublithic to lithic arenite and quartz arenite; subordinate shale and siltstone; crossbedding and ripple marks are common, mudcracks and synaeresis cracks locally developed.|03-APR-12
7009|Gardiner Sandstone|62377|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Overlies: Mount Charles Formation.||||||07-NOV-08
7009|Gardiner Sandstone|62580|6|Mentioned|p25|||Unconformably overlies Nora Range Monzogranite.||||||07-FEB-11
7009|Gardiner Sandstone|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Birrindudu Group. Geological Province: Birrindudu Basin. Sandstone, sublithic arenite, quartz arenite, conglomerate, siltstone and shale.||||||07-NOV-08
7009|Gardiner Sandstone|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Coarse grained silty sandstone, heavily quartz veined; veins contain some quartzite.||||||23-DEC-09
7009|Gardiner Sandstone|63261|5|Briefly described|p7, p9 Fig. 5, p17|||Of Birrindudu Group. Unconformably overlies Pargee Sandstone. Thickness: 1000m. Geological province: Victoria-Birrindudu Basin.||||||07-FEB-11
7009|Gardiner Sandstone|63866|5|Briefly described|p92, p99|||Birrindudu Basin.||||Overlain by the Limbunyah Group.||
7009|Gardiner Sandstone|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Of Birrindudu Group. Age: 1735-1640Ma. Geol Prov: Birrindudu Basin. Undivided; cross-bedded sandstone and quartz sandstone, siltstone, shale, and conglomerate; glauconitic sandstone; minor dolomitic sandstone.||||||
7009|Gardiner Sandstone|64329|5|Briefly described|p20|||Unconformably overlies Killi Killi beds. Thorium-uranium prospects in the minerlisation at base of unit.||||||05-AUG-08
7009|Gardiner Sandstone|64572|5|Briefly described|p814|Paleoproterozoic|Paleoproterozoic|Age: ca 1630Ma. Geological Province: Birrindudu Basin.||||||22-DEC-08
7009|Gardiner Sandstone|64662|5|Briefly described|p30 Fig. 3, p40-41, 43|Statherian|Statherian|Basal Birrindudu Group. Age: ~1.77 - 1.64 Ga, for same reasons as unconformably underlying Pargee Sandstone. Tanami region.||||||07-FEB-11
7009|Gardiner Sandstone|64675|6|Mentioned|Fig.6, Fig.18, Fig.19, p15, Fig.25|||||Of the Birrindudu Group.||Unconformably underlain by the Browns Range Metamorphics, MacFarlane Peak Group, and Coomarie Suite||
7009|Gardiner Sandstone|64733|6|Mentioned|p172 Fig.4, p173|Statherian|Statherian|||Of Birrindudu Group.||Unconformably overlies Pargee Sandstone.||20-APR-12
7009|Gardiner Sandstone|64737|5|Briefly described|p232 Fig.2, p233-4, p236 Tab.4, p243||Statherian|Detrital zircon ages dominated by 1840-1800 Ma. Younger than Pargee Group (i.e. <1768 +/- 14 Ma).|1768 +/- 14 Ma to 1742 +/- 50 Ma.|Base of Birrindudu Group.||||01-MAY-12
7009|Gardiner Sandstone|64956|5|Briefly described|p7|||Rocks are typically pink to grey, fine- to medium-grained, thinly to medium bedded, planar laminated to cross-bedded quartz arenite to sublithic arenite, with shale clasts.||||||07-FEB-11
7009|Gardiner Sandstone|65074|4|Described|p349, p351 fig 4-37, p354 Tb. 4-11, p352|Mesoproterozoic|Mesoproterozoic|Named after Gardner [sic] Range. Oldest unit in (North/Centre) Birrindudu Basin. Type section: Larranganni Bluff. 2200m thick. K-Ar and Rb-Sr age on glauconite.|1560 Ma (Blake et al., 1979).|Birrindudu Group||Unconformably overlies Mount Winnecke Formation, Supplejack Downs and Pargee Sandstones. Overlain by Talbot Well Formation (conformably). Probably equivalent to Limbunya Group and McArthur Group (NT)|White to purple sublithic arenite, shale; minor quartz arenite, conglomerate, siltstone, glauconitic and dolomitic sandstone.|
7009|Gardiner Sandstone|65232|5|Briefly described|p78|||Unconformity at base. Geol. Prov: Tanami Region. Of Birrindudu Group?||||||09-FEB-10
7009|Gardiner Sandstone|65323|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; underlies the Talbot Well Formation; shown as lateral equivalent/interfingering with Supplejack Downs Sandstone;includes the informal Glauconitic Sandstone member which is not present on map||||||12-DEC-12
7009|Gardiner Sandstone|65324|5|Briefly described|Map legend|Statherian|Statherian|Of Birrindudu Group; underlies Talbot Well Formation; shown as lateral equivalent/interfingering with Supplejack Downs Sandstone; includes informal Glauconitic Sandstone member.|||||Sandstone: white, sublithic arenite, quartz arenite, conglomerate, siltstone, shale; thin to thick bedded, medium-coarse grained, poorly sorted|12-DEC-12
7009|Gardiner Sandstone|65326|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; shown as lateral equivalent/interfingering with  the Talbot Well Formation; includes the informal Glauconitic Sandstone member which is not shown on map||||||12-DEC-12
7009|Gardiner Sandstone|65327|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
7009|Gardiner Sandstone|65328|5|Briefly described|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||12-APR-10
7009|Gardiner Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Birrindudu Group.||Unconformably overlies Inverway Metamorphics. Is overlain by Talbot Well Formation.||
7009|Gardiner Sandstone|65349|5|Briefly described|Map legend|Statherian|Statherian|Of Birrindudu Group; underlies Talbot Well Formation;  shown as lateral equivalent/interfingering with Supplejack Downs Sandstone; includes informal Glauconitic Sandstone member. Sandstone: white, sublithic arenite, quartz arenite, conglomerate, siltstone, shale; thin to thick bedded, medium-coarse grained, poorly sorted||||||12-DEC-12
7009|Gardiner Sandstone|65350|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
7009|Gardiner Sandstone|65351|6|Mentioned|Map legend|Statherian|Statherian|Not shown on map; of the Birrindudu Group||||||
7009|Gardiner Sandstone|65352|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; only non-magnetic sandstone shown on map; underlies the Talbot Well Formation; shown as lateral equivalent/interfingering with Supplejack Downs Sandstone; includes the informal Glauconitic Sandstone member which is not present on map||||||12-DEC-12
7009|Gardiner Sandstone|65353|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; underlies the Talbot Well Formation;  shown as lateral equivalent/interfingering with Supplejack Downs Sandstone;includes the informal Glauconitic Sandstone member which is not present on map||||||12-DEC-12
7009|Gardiner Sandstone|65354|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; underlies the Talbot Well Formation; shown as lateral equivalent/interfingering with Supplejack Downs Sandstone; includes the informal Glauconitic Sandstone member (not shown on map)||||||12-DEC-12
7009|Gardiner Sandstone|65355|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; non- to weakly magnetic sandstone; only non-magnetic sandstone shown on map; underlies the Talbot Well Formation;  shown as lateral equivalent/interfingering with Supplejack Downs Sandstone; includes the informal Glauconitic Sandstone member which is not present on map||||||12-DEC-12
7009|Gardiner Sandstone|65356|5|Briefly described|Map legend|Statherian|Statherian|Of the Birrindudu Group; only non-magnetic sandstone shown on this map; underlies the Talbot Well Formation; shown as lateral equivalent/interfingering with Supplejack Downs Sandstone;  includes the informal Glauconitic Sandstone member which is not present on map||||||12-DEC-12
7009|Gardiner Sandstone|66129|6|Mentioned|p216 Fig.3|||In Birrindudu Group.||||||
7009|Gardiner Sandstone|66468|6|Mentioned|p24 Fig.7|||In Birrindudu Group.||||||
7009|Gardiner Sandstone|67127|5|Briefly described|p109, p111, p168, p175|Mesoproterozoic|Mesoproterozoic|Victoria-Birrindudu basins. Associated with the Killi Killi Hills Uranium REE prospect. Halls Crek, Birrindudu Basin. Xenotime features high concentrations of yttrium and phosphorous.||||Unconformably overlies the the Killi Killi Formation.||
7009|Gardiner Sandstone|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||||Coarse-grained silty sandstone, heavily quartz-veined, veins contain some turquoise.|
7009|Gardiner Sandstone|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Includes a glauconitic sandstone unit.||Unit in Birrindudu Group.||Unconformably overlies Tanami Group, Pargee Sandstone, Coomarie Suite and Mount Charles Formation. Is overlain by Talbot Well Formation.||13-JAN-12
7009|Gardiner Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Statherian|Statherian|Birrindudu Basin|||||Cross bedded, white, medium- to coarse-grained, poorly sorted quartz sandstone with siltstone, mudstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent.|
7009|Gardiner Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Statherian|Statherian|Birrindudu Basin||Birrindudu Group|Includes unnamed siltstone and mudstone member||Cross bedded, white, medium- to coarse-grained, poorly sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent|31-JUL-15
7009|Gardiner Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Cross bedded, white, medium to coarse grained, poorly sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone and basal conglomerate.|
7009|Gardiner Sandstone|69425|6|Mentioned|p10:4|||Mentioned as possible correlative of Hatches Creek Group, based on geochronological grounds.||||||12-JUL-16
7009|Gardiner Sandstone|69426|5|Briefly described|p11:5 Fig.11.4. 11:10, 14, 27-28, 36|||In Blake et al. (1979). Minor occurrences of uranium are noted along the underlying unconformity.||Birrindudu Group.||Unconformably overlies Pargee Sandstone, Killi Killi Formation and Mount Charles Formation.||12-JUL-16
7009|Gardiner Sandstone|69432|4|Described|p17:2-5, 14|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Includes the former Supplejack Downs Sandstone (Blake et al., 1975). Forms prominent ridges. Up to c.3000m thick. Basal conglomerate hosts two uranium and rare earth prospects (Killi Killi Hills 1 and 2). Minimum age, from diagenetic xenotime growth; probably contemporaneous with deposition of the Limbunya Group.|>1632 +/- 3 Ma (Vallini et al., 2007).|Birrindudu Group.||Unconformably overlies Mount Charles Formation. Is overlain unconformably by the Lothari Hill Sandstone.|Medium- to thickly-bedded sublithic to lithic sandstone and quartz sandstone; shale and siltstone are subordinate; conglomerate and pebbly sandstone lenses locally occur throughout the unit. Glauconitic sandstone occurs in upper levels.|12-JUL-16
7009|Gardiner Sandstone|69587|4|Described|GEOL_LUT_CSV files|Statherian|Statherian|Geological province: North Australian Craton. Of Birrindudu Basin. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.|1735-1640 Ma (inferred)|Unit of Birrindudu Group.|||Cross bedded, white, medium- to coarse-grained, poorly sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent|
7009|Gardiner Sandstone|69618|6|Mentioned|p96 Fig.6|||Tanami goldfield.||||||
7009|Gardiner Sandstone|69634|5|Briefly described|100k_interpgeop_lut.csv|Statherian|Statherian||1735-1640 Ma (Inferred)|Unit of Birrindudu Group.|||Cross bedded, white, medium- to coarse-grained, poorly sorted (micaceous) quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent|
7009|Gardiner Sandstone|69673|6|Mentioned|p48 fig 35|||||Birrindudu Group||Overlain by Talbot Well Formation||
7009|Gardiner Sandstone|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.|||Cross-bedded, white, medium- to coarse-grained, poorly-sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent.|
7009|Gardiner Sandstone|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Shallow marine to emergent. Two facies are mapped separately: sandstone, dolomitic sandstone and siltstone; and siltstone and mudstone, minor fine-grained micaceous quartz sandstone.||Birrindudu Group.||Overlies Killi Killi Formation.|Cross-bedded, white, medium- to coarse-grained, poorly sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate.|
7009|Gardiner Sandstone|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Unclear if age range refers to the Group or just the Gardiner Sandstone.|1735-1640 Ma.|Birrindudu Group.|||Cross-bedded, white, medium- to coarse-grained, poorly sorted quartz sandstone with siltstone and shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate; shallow marine to emergent.|
7009|Gardiner Sandstone|70154|4|Described|100k_interpgeop_lut.csv|Statherian|Statherian||1640-1735 Ma||||Cross bedded, medium-coarse grained, poorly sorted quartz sandstone and with siltstone and shale, minor glauconitic sandstone with flaggy dolomitic sandstone and basal conglomerate. Mudstone and thin bedded sandstone.|
7009|Gardiner Sandstone|70291|4|Described|p180,194|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Maximum depositional age ~1815 Ma [which seems to exceed that of Birrindudu Group? See Table 1 p180]. |~1815 Ma|Unit of Birridudu Group.|||Sublithic to lithic sandstone and quartz arenite, with lesser shale and siltstone and basal conglomerate|
7009|Gardiner Sandstone|70478|5|Briefly described|p11|Orosirian|Paleoproterozoic|The highly magnetic rocks are probable correlatives of Tanami Group stratigraphy. Underlain by Grimwade Suite granite in borehole TAN99DDH21. Nature of noundary not discussed.|||||Arkosic-lithic sandstone.|11-OCT-19
7009|Gardiner Sandstone|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.||Is overlain by Talbot Well Formation.|Quartz sandstone, conglomerate, pebbly red sandstone (siltstone clasts), sublithic quartz sandstone, siltstone and shale; minor glauconitic sandstone.|
7009|Gardiner Sandstone|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Birrindudu Group.|||Sublithic sandstone, quartz sandstone, conglomerate, siltstone and shale.|
7009|Gardiner Sandstone|71267|4|Described|GEOL_LUT_CSV files|Statherian|Statherian|Geological province: Granites-Tanami Orogen. Of Birrindudu Basin. Event: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1735-1640 Ma (inferred)|Unit of Birrindudu Group.||Underlain unconformably by Browns Range Metamorphics.|Shallow marine to emergent, cross bedded, thinly to thickly bedded white sublithic medium to coarse grained, poorly sorted quartz sandstone with siltstone, shale; minor glauconitic sandstone and flaggy dolomitic sandstone, and basal conglomerate|
7009|Gardiner Sandstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||||||
7009|Gardiner Sandstone|71348|5|Briefly described|p217|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami Region, North Australian Craton. Maximum depositional age c. 1780 Ma Maidment et al., 2005; Cross and Crispe, 2007; Hollis et al., 2013; Kositcin et al., 2015).|< 1780 Ma.|||||
7009|Gardiner Sandstone|71349|5|Briefly described|p723-727, p731-733, p736|||Detrital zircon analyses detailed; provenance discussed. Zircon age range from c.2.6 to c.1.8 Ga. Minimum age of c.1.63 Ma inferred from diagenetic xenotime growth (Vallini et al., 2007).||Basal Birrindudu Group.||Unconformably overlies Browns Range Metamorphics.|Medium-grained, sub-lithic to lithic arenite and quartz arenite; subordinate shale and siltstone units; a thin basal conglomerate commonly occurs.|23-OCT-18
7009|Gardiner Sandstone|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1812+/-18 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz arenite.|
7009|Gardiner Sandstone|72071|5|Briefly described|p1298|Paleoproterozoic|Paleoproterozoic|Unmetamorphosed.|ca. 1.66-1.64 Ga|Unit of Birridudu Group.||||
7009|Gardiner Sandstone|73089|4|Described|p: 6-7, 9, 11, 13, 15-16, 29-30, 33, 44|Statherian|Statherian|Birrindudu Basin, lowermost unit. 3 km thick. Shallow marine to emergent depositional setting. Secondary xenotime age of 1632 +/- 3 Ma (U-Pb). Geochron sandstone sample numbers = GA 2001082010 and GA 2001082516 [see report for geochon details; authors didn't find youngest population that was reported in other studies]. Possibly derived from the Granites-Tanami Orogen; contains detrital zircon age components that appear to reflect reworking of the underlying Tanami Group.|1768-1632 Ma|||Unconformably underlain by Pargee Sandstone.|Cross-bedded, thinly to thickly bedded sublithic arenite, quartz arenite, conglomerate, shale, siltstone, glauconitic sandstone.|
7044|Gascoyne Complex|14228|6|Mentioned|p2, p10|Paleoproterozoic|Paleoproterozoic|||||||
7044|Gascoyne Complex|22437|5|Briefly described|p853|||||||||
7044|Gascoyne Complex|22660|4|Described|p 300||Paleoproterozoic|The high-grade metamorphic core of the Capricorn Orogen, p300.||||||07-NOV-08
7044|Gascoyne Complex|22716|5|Briefly described|table4,fig2,p227,229|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|22743|6|Mentioned|p509|||||||||
7044|Gascoyne Complex|22771|6|Mentioned|Fig12.2p38|||||||||
7044|Gascoyne Complex|22814|6|Mentioned|p259|||||||||
7044|Gascoyne Complex|22816|6|Mentioned|p15 Fig.7|||||||||
7044|Gascoyne Complex|22905|6|Mentioned|p53|||Unconformably overlain by Edmund Group.||||||
7044|Gascoyne Complex|22940|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|23156|6|Mentioned|p8|Proterozoic|Proterozoic|Previously known as Gascoyne Province.||||||
7044|Gascoyne Complex|23205|6|Mentioned|p425, Fig.4|||of Capricorn Orogen||||||
7044|Gascoyne Complex|23403|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|23485|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Geological Province: Capricorn Orogen.||||||07-NOV-08
7044|Gascoyne Complex|23486|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|23487|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|23525|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 2550-1970Ma||||||07-NOV-08
7044|Gascoyne Complex|23529|5|Briefly described|p6|||||||||
7044|Gascoyne Complex|23589|6|Mentioned|p6|||||||||
7044|Gascoyne Complex|23592|5|Briefly described|p12|Paleoproterozoic|Archean|Geological Province: Capricorn Orogen.||||||07-NOV-08
7044|Gascoyne Complex|23620|4|Described|p3|Paleoproterozoic|Paleoproterozoic|Granodiorite, monzogranite, granite, and pegmatite: includes dolerite and gabbro.  See also p4 Fig. 2.||||||07-NOV-08
7044|Gascoyne Complex|23723|5|Briefly described|p5|||||||||
7044|Gascoyne Complex|23744|6|Mentioned|p3|||||||||
7044|Gascoyne Complex|23773|5|Briefly described|p751|||||||||
7044|Gascoyne Complex|23774|5|Briefly described|p731|||In the Capricorn Orogen.||||||
7044|Gascoyne Complex|23780|5|Briefly described|p42|Paleoproterozoic|Paleoproterozoic|Overlying Unit: Mount James Formation (unconformable).||||||07-NOV-08
7044|Gascoyne Complex|23781|5|Briefly described|p1|Paleoproterozoic|Archean|||||||07-NOV-08
7044|Gascoyne Complex|23976|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
7044|Gascoyne Complex|23977|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
7044|Gascoyne Complex|23978|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
7044|Gascoyne Complex|24041|5|Briefly described|p492 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|24114|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Geological Province: Yilgarn Craton.||||||07-NOV-08
7044|Gascoyne Complex|24115|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Overlain by the Edmund Group.||||||
7044|Gascoyne Complex|24183|5|Briefly described|p2 Fig.1, p6|Paleoproterozoic|Paleoproterozoic|Geological Province: Capricorn Orogen. Age: 1797 +/- 8 Ma.||||||07-NOV-08
7044|Gascoyne Complex|24332|5|Briefly described|p134, p144|||||||||
7044|Gascoyne Complex|24410|6|Mentioned|p133 Fig. 78|||||||||
7044|Gascoyne Complex|24522|6|Mentioned|p78, p79 Fig. 1a|Paleoproterozoic|Neoarchean|||||||07-NOV-08
7044|Gascoyne Complex|24526|6|Mentioned|p114|||||||||
7044|Gascoyne Complex|24535|5|Briefly described|p2|Statherian|Statherian|Age of constituent monzongranite: 1619+/-15 Ma.||||||
7044|Gascoyne Complex|24544|5|Briefly described|p5|||Granite plutons, sheets and dykes; granitic gneiss; and metasedimentary rocks.||||||
7044|Gascoyne Complex|24602|5|Briefly described|p853, p862|||||||||
7044|Gascoyne Complex|42148|6|Mentioned|p685|||||||||
7044|Gascoyne Complex|42260|6|Mentioned|p7|||||||||
7044|Gascoyne Complex|42278|6|Mentioned|p42|||||||||
7044|Gascoyne Complex|42441|6|Mentioned|p88|||? Structural term.||||||
7044|Gascoyne Complex|42730|5|Briefly described|p15|||||||||
7044|Gascoyne Complex|43561|6|Mentioned|p1435|||||||||
7044|Gascoyne Complex|43697|6|Mentioned|Fig.1, p26|||||||||08-AUG-05
7044|Gascoyne Complex|44109|6|Mentioned|p165 Fig. 163|||||||||
7044|Gascoyne Complex|44111|6|Mentioned|p56 Fig.1|||||||||
7044|Gascoyne Complex|44141|6|Mentioned|p308|||Source of granitoid detritus in conglomerates of Bresnahan Group.||||||
7044|Gascoyne Complex|44142|5|Briefly described|p311, p320-321, p324-325|||See also p326-327 Tb.4-5, p329. Block faulting in the Gascoyne Complex basement initiated the Bangemall Group sedimentation.||||Overlain unconformably by Edmund Subgroup.|High-grade metamorphic and plutonic igneous rocks.|13-MAR-18
7044|Gascoyne Complex|44151|6|Mentioned|p159 Fig.2-145|||||||||
7044|Gascoyne Complex|49896|6|Mentioned|p6|||Of the Capricorn Orogen.||||||
7044|Gascoyne Complex|50008|5|Briefly described|p43|Paleozoic|Paleozoic|Age of zircon populations given. May be source area for Tarcunyah Group.||||||07-NOV-08
7044|Gascoyne Complex|50026|6|Mentioned|p11|||Structural term in this context.||||||18-NOV-04
7044|Gascoyne Complex|50216|5|Briefly described|p205|Paleoproterozoic|Paleoproterozoic|Structural term in this context. Age: 2550-1620 Ma.||||||07-NOV-08
7044|Gascoyne Complex|50217|5|Briefly described|p220|||Previously recognised as a single crustal domain, this has now been informally subdivided into northern and southern parts separated by the 1840-1800 Ma Minnie Creek Batholith, that is the Southern and Northern Gascoyne Complexes.||||||
7044|Gascoyne Complex|50218|5|Briefly described|p238 Fig. 1, p239|Paleoproterozoic|Archean|Major tectonic unit within the Capricorn Orogeny; southern part referred to as Glenburgh Terrane - term used in a structural sense also. Age: 2550-1970Ma.||||||07-FEB-11
7044|Gascoyne Complex|50219|5|Briefly described|p259||Paleoproterozoic|Consists mainly of medium- to high-grade metamorphic rocks intruded by large batholiths of granite.  Mainly a structural term in this context.||||||07-FEB-11
7044|Gascoyne Complex|50220|6|Mentioned|p279|||||||||
7044|Gascoyne Complex|50221|5|Briefly described|p296 Fig.1|Paleoproterozoic|Paleoproterozoic|Structural term in this context. Age: 2500-1800 Ma.||||||07-NOV-08
7044|Gascoyne Complex|50222|5|Briefly described|p316 Fig. 1, p317|||Structural term in this context.||||||
7044|Gascoyne Complex|50223|5|Briefly described|p344 Fig. 1, p356||Paleoproterozoic|||||||07-NOV-08
7044|Gascoyne Complex|50225|5|Briefly described|p385|||Unconformably overlain by Bangemall Supergroup.||||||07-FEB-11
7044|Gascoyne Complex|50226|4|Described|p417-418,p427 Fig. 6|Paleoproterozoic|Paleoproterozoic|Granitic gneisses, metasedimentary rocks (Morrisey Metamorphic Suite of Williams, 1986), and large plutons of tonalite through to syenogranite (including part of Minnie Creek Batholith).  Unconformably overlain by Edmund Group (Bangemall Basin).||||||07-NOV-08
7044|Gascoyne Complex|50228|5|Briefly described|p492|||||||||
7044|Gascoyne Complex|50313|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Structural term in this context.  Age: >1800Ma.||||||07-NOV-08
7044|Gascoyne Complex|50323|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Moorarie Supersuite.||||||07-NOV-08
7044|Gascoyne Complex|50333|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic|Part of the Capricorn Orogen.  Includes the Glenburgh Terrane in the southern part of the complex.||||||07-NOV-08
7044|Gascoyne Complex|50425|5|Briefly described|p2.1|||Intruded by: Chararoo Supersuite, Minnie Creek Supersuite.||||||
7044|Gascoyne Complex|50543|5|Briefly described|Map|||Structural term in this context.||||||
7044|Gascoyne Complex|50620|6|Mentioned|p200 Fig. 8|||Of the Capricorn Orogeny.||||||
7044|Gascoyne Complex|60470|6|Mentioned|p2, 8|Paleoproterozoic|Paleoproterozoic|One possible source area for Gunanya Sandstone. ||||||
7044|Gascoyne Complex|60694|6|Mentioned|p274|||Geological Province: Yilgarn Craton.||||||12-JAN-05
7044|Gascoyne Complex|61064|5|Briefly described|p12, p42, p46|Paleoproterozoic|Paleoproterozoic|Geological Province: Capricorn Orogen.||||||07-NOV-08
7044|Gascoyne Complex|61262|4|Described|p443, p458 App.|||Structural term in this context.||||||
7044|Gascoyne Complex|61563|6|Mentioned|p577 Fig. 1|||Structural term in this context.||||||
7044|Gascoyne Complex|61564|6|Mentioned|p589 Fig. 1|||Structural term in this context.||||||
7044|Gascoyne Complex|61850|5|Briefly described|p323, p324 Fig. 1|Proterozoic|Archean|Metamorphic rocks including granitoids, gneiss, metamorphosed siliciclastic and calc-silicate rocks, and amphibolite.  Overlain by the Bangemall Supergroup.||||||07-NOV-08
7044|Gascoyne Complex|62428|5|Briefly described|p336|Paleoproterozoic|Paleoproterozoic|Metamorphic and granitoid rocks.||||||10-FEB-09
7044|Gascoyne Complex|63246|5|Briefly described|p477|||Overlain by Bangemall Supergroup. Low + high grade metamorphic rocks, granites and pegmatites of Capricorn Orogen, namely metasedimentary schists of Morrissey and Pooranoo Metamorphics. Comprises several E-SE trending structural and metamorphic zones.||||||
7044|Gascoyne Complex|63869|5|Briefly described|p1, p2, p4, p5, p9-20, p24, p28, p29|Paleoproterozoic|Paleoproterozoic|See also p38, p43, p44, p46-48, p49, p52, p56-60, Plate 1. Capricorn Orogen. [used in a 'geological province' sense] Deformed, metamorphosed and intruded by granites between 1830-1780 Ma. A variety of mineral deposits are decribed.||||Intruded by Moorarie and Durlacher Supersuites. Is overlain by Edmund Group.|Metasedimentary and meta-igneous rocks; granites.|06-MAR-18
7044|Gascoyne Complex|64161|6|Mentioned|p578 Fig.1, p590, p591 Fig.11, p592-593|Statherian|Neoarchean|Plutonic rocks and medium to high-grade metasedimentary rocks. 2550-1620 Ma||||||
7044|Gascoyne Complex|64287|6|Mentioned|p31|||Probably a structural term?||||||07-FEB-11
7044|Gascoyne Complex|64384|6|Mentioned|p3, p45, p81|||Comprises high grade metamorphic and igneous rocks.||||||07-FEB-11
7044|Gascoyne Complex|64572|5|Briefly described|p798, p806, p814, p807 Fig. 9|Neoproterozoic|Neoproterozoic|Age: 954+/-12Ma (SHRIMP) from a monzonite and by Rb-Sr ages ca 980 and ca 940Ma.||||||22-DEC-08
7044|Gascoyne Complex|64573|6|Mentioned|p788|Paleoproterozoic|Paleoproterozoic|Monzogranitic and subordinate metasedimentary rocks variably deformed.||||||07-FEB-11
7044|Gascoyne Complex|64635|6|Mentioned|p2 Fig.1|||||||||
7044|Gascoyne Complex|64722|5|Briefly described|p7|Statherian|Neoarchean|Structural unit? Medium to high grade metamorphic rocks. Age of 2550 - 1620 Ma given after Sheppard (2007).||||||11-APR-12
7044|Gascoyne Complex|64728|4|Described|p93, p95, pp106-109.|Paleoproterozoic|Paleoproterozoic|Igneous and metamorphic rocks. Intruded by granites of the Moorarie Supersuite and of the later, c.1620 Ma, Durlacher Supersuite. Probable main source area, along with Pilbara Craton, for sediments of Bangemall Supergroup.|c.1830-1620 Ma.||Includes Bertibubba and Dalgaringa Supersuites.|Is unconformably overlain by Bangemall Supergroup.||
7044|Gascoyne Complex|64777|6|Mentioned|p6-8|Palaeoproterozoic|Palaeoproterozoic|Capricorn Orogen.|||||Plutonic and medium- to high-grade metamorphic rocks.|
7044|Gascoyne Complex|65152|6|Mentioned|p1-3.|Paleoproterozoic|Archean|Used as a structural term in this article.||||||
7044|Gascoyne Complex|65472|6|Mentioned|p1|||||||||
7044|Gascoyne Complex|65506|5|Briefly described|p986-987, p996-997, p999|1780 Ma.|1830 Ma.|Subduction-related granitic rocks and metamorphic rocks. Capricorn Orogen. Is overlain unconformably by Bangemall Supergroup.||||||
7044|Gascoyne Complex|65692|5|Briefly described|p1,p7-8, p23, p29-30, p53, p56, p65, p68|Paleoproterozoic|Neoarchean|West Capricorn Orogen. Collision of the SW part of this Complex with the NW Yilgarn Craton is thought to be recorded in the 2005-1960 Ma Glenburgh Orogeny. Extensively reworked in the N by the 1680-1620 Ma Mangaroon Orogeny, and in central parts by the 1030-950 Ma Edmundian Orogeny. Hf values suggest Archean units may have been a sediment source for Earaheedy Basin.|2550-1620 Ma.|||||
7044|Gascoyne Complex|65830|3|Fully described|p1-4, p10, p12, p18-22, p24-28, p35|Statherian|Statherian|See also p38-39. Includes granite from the Durlacher Supersuite and metasedimentary rocks from the Pooranoo Metamorphics.|~1680-1620 Ma||Includes Durlacher Supersuite, Pooranoo Metamorphics, Moorarie Supersuite, Morrissey Metamorphics, Dalgaringe Supersuite, Moogie Metamorphics, Halfway Gneiss.|Overlain by the Bangemall Supergroup. Overlain by the Yilgatherra Formation. Unconformably overlain by the Mount Augustus Sandstone. Intruded by the Durlacher Supersuite.|Foliated, medium- to coarse-grained biotite-muscovite monzogranite, and siliciclastic metasedimentary rocks.|
7044|Gascoyne Complex|66106|6|Mentioned|p27, 45|||||||||
7044|Gascoyne Complex|66107|5|Briefly described|p4 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Granite, medium to high grade metamorphics.|
7044|Gascoyne Complex|66427|6|Mentioned|p40 Fig.1, p41 Tb.1, p49, p70, p72-73|||||||||
7044|Gascoyne Complex|66882|6|Mentioned|p101 Fig.1, p116, p118|||||||||
7044|Gascoyne Complex|66950|6|Mentioned|p1|||The use of the term Gascoyne Complex is discontinued in discussing orogenesis, because complex is a lithostratigraphic term; therefore, the crustal-volume term Gascoyne Province is reinstated.||||||16-DEC-16
7044|Gascoyne Complex|67200|6|Mentioned|p56||||||||Granite.|
7044|Gascoyne Complex|67855|4|Described|p197-9, 202, 203, 210, 221, 223|||Used in a 'geological province' sense. Divided into 5 main zones: A 3.7-3.3 Ga Narryer Gneiss Complex, B Interleaved basement and cover (including Morrissey Metamorphic Suite), C mantled-gneiss domes (eg Yinnetharra Gneiss Dome), D Minnie Creek batholith, E Granitoid plutons and metasedimentary rocks (metamorphosed Morrissey metamorphics).|||||Complex.|
7044|Gascoyne Complex|69166|6|Mentioned|148969.1.pdf|Paleoproterozoic|Paleoproterozoic|Age derived from monzogranite sample (169053.1.pdf)|1635 Ma +/- 15 ma (SHRIMP)||Includes Durlacher Supersuite||Leucocratic gneiss and coarse grained monzogranite, biotite-muscovite monzogranite. Leucocratic tonalite dykes.|
7044|Gascoyne Complex|73214|6|Mentioned|p974 Fig.1|Archean|Archean|||||||
7072|Gearle Siltstone|12471|5|Briefly described|p475.|Cenomanian|Albian|Has a variable, low velocity, shallow gas zone causing time-pushdowns and masking the low amplitude closure in underlying, Lower Cretaceous targets. See also Figs 3, 4.||Unit in Winning Group.||Overlies Windalia Radiolarite. Is overlain by Toolonga Calcilutite.||27-OCT-14
7072|Gearle Siltstone|12491|5|Briefly described|p457, pp459-462, pp464-468|Cretaceous|Cretaceous|Deposited on shelf-slope to deep water environment; slumping and channelling can be seen on seismic data. Gearle Formation and Gearle Siltstone used interchangeably in text and figures.||||Overlies Windalia Radiolarite.|Thick sequence of siltstones and shales.|20-JAN-15
7072|Gearle Siltstone|12729|6|Mentioned|p.15, 34||Cretaceous|||Winning Group||Overlies the Windalia Radiolarite, coeval with the Alinga Formation.|Glauconitic siltstone.|
7072|Gearle Siltstone|13615|3|Fully described|p4-5, p6-8, p11-12, p101 App. 3, p118|Turonian|Albian|Peedamullah Shelf. Mostly <200m thick, more than 500m thick offshore. Spores/Pollen Zone and Dinoflagellate zones provided. Small gas accumulations imaged in this unit. Type section is found in C-Y Creek, Giralia Anticline; 22def44'S 114deg09'E. Age derived from fossil assemblage of foraminifers, bivalves and belemnites. Deposited in a shallow marine, low energy and restricted environment. See also p18-p20, p25, p29-p31, p34-p35, p38-p39, p41-p42, p49, p51-p52, p54, p56, p58, p63-p64, p66-p72, p81, p83, p118,  Plates 2, 3.||Winning Group||Conformably overlies the Windalia Radiolarite. Disconformably overlain by the Toolonga Calcilutite, Cardabia Group and Trealla Limestone.|Clayey siltstone, dark grey-black claystone, radiolarian siltstone.|07-FEB-19
7072|Gearle Siltstone|14228|5|Briefly described|p5 fig 2, p9, p26|Cenomanian|Albian|Locally records an internal hiatus up to c.15 m.y.||Winning Group||Overlies Windalia Radiolarite.|Dark grey to black siltstone, pyritic, soft; glauconitic.|
7072|Gearle Siltstone|22703|4|Described|p115,118-9,Fig.3|Cenomanian|Aptian|||||||
7072|Gearle Siltstone|23311|5|Briefly described|map legend|Late Cretaceous|Early Cretaceous|Of Winning Group.||||||
7072|Gearle Siltstone|23312|5|Briefly described|map legend|Late Cretaceous|Early Cretaceous|Winning Group.||||||
7072|Gearle Siltstone|23355|5|Briefly described|8 Fig.1|Late Cretaceous|Early Cretaceous|||||||
7072|Gearle Siltstone|23379|4|Described|p158-161,164-165,168-174|Turonian|Albian|Comprises the informal Upper Gearle Siltstone and Lower Gearle Siltstone. of Barrow Sub-basin, Carnarvon Basin.||||||
7072|Gearle Siltstone|23403|4|Described|p9|Late Cretaceous|Early Cretaceous|Of Winning Group.||||||24-NOV-09
7072|Gearle Siltstone|23433|5|Briefly described|p111|||||||||
7072|Gearle Siltstone|23535|6|Mentioned|Figure 3 p127.|||Geological Province: Carnarvon Basin.||||||
7072|Gearle Siltstone|23572|4|Described|p12|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Underlying Unit: Windalia Sandstone Member.||||||
7072|Gearle Siltstone|23726|5|Briefly described|p69|Late Cretaceous|Early Cretaceous|Overlying unit Toolonga Calcilutite. Underlying unit Windalia Radiolarite. Geological Province: Carnarvon Basin.||||||
7072|Gearle Siltstone|23815|4|Described|p297|Turonian|Albian|Geological Province: Carnarvon Basin. Overlying units: Toolonga Calcilutite and Korojon Calcarenite (both disconformable). Underlying unit: Windalia Radiolarite (confromable). Max thickness: 346 m. Fossiliferous.||||||
7072|Gearle Siltstone|23915|5|Briefly described|p518, 519 Table 1|Cenomanian|Albian|Overlies: Windalia Radiolarite (disc). Underlies: Toolonga Calcilctite (disc).  Max. Thickness: ~120m.  Geological Province: Southern Carnarvon Basin.||||||
7072|Gearle Siltstone|23935|4|Described|p11 Fig.7, p12 Fig.8|Turonian|Albian|Of Winning Group. Disconformably overlies Windalia Radiolarite. Unconformably overlain by Toolonga Calcilutite. Dark-grey to black pyritic mudstone and siltstone. Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
7072|Gearle Siltstone|24059|5|Briefly described|p132|Cretaceous|Cretaceous|Geological Province: Barrow Sub-basin.||||||
7072|Gearle Siltstone|24084|5|Briefly described|p146 Fig.2|Late Cretaceous|Early Cretaceous|Geological Province: North Carnarvon Basin.||||||16-MAR-05
7072|Gearle Siltstone|24160|5|Briefly described|p36, 38, 39|Cretaceous|Cretaceous|Carnarvon Basin. Type section is in C-Y Creek in the Giralia Anticline. Thickness >700 m. Hosts bentonite deposits.||Winning Group||Overlies Windalia Radiolarite conformably; grades laterally into Alinga Formation and Haycock Marl. Is overlain conformably by Toolonga Calcilutite.|A silty and clayey sequence with appreciable radiolarian siltstone. Dark grey to black with a sulfurous odour. Clay horizons are bentonitic, siltstone horizons are pyritic, glauconitic or micaceous. Contains bedded barite and gypsum.|
7072|Gearle Siltstone|24205|5|Briefly described|p248, p253|||Overlies the Muderong Shale.  Geological Province: Northern Carnarvon Basin.||||||
7072|Gearle Siltstone|24331|5|Briefly described|p475 Fig.2|Late Cretaceous|Early Cretaceous|Conformably overlies Windalia Radiolarite. Unconformably overlain by Toolonga Calcilutite. Marine. Geological Province: Barrow Sub-basin.||||||
7072|Gearle Siltstone|24351|5|Briefly described|Plate 4 (in pocket)|Late Cretaceous|Early Cretaceous|Of the Winning Group. Geological Province :Exmouth Plateau, Exmouth Sub-basin, Gascoyne Platform/Sub-basin.||||||13-DEC-07
7072|Gearle Siltstone|29381|4|Described|p67|||||||||
7072|Gearle Siltstone|29721|6|Mentioned|Table 102|||||||||
7072|Gearle Siltstone|30016|6|Mentioned|p92|||||||||
7072|Gearle Siltstone|30110|6|Mentioned|p81|||Cretaceous - Albian to Coniacian age.Part of the Winning Group.||||||
7072|Gearle Siltstone|30304|4|Described|p53|||Albanian to Turonian age||||||
7072|Gearle Siltstone|30365|6|Mentioned|Fig.8|||||||||
7072|Gearle Siltstone|31083|6|Mentioned|p455|||||||||
7072|Gearle Siltstone|31561|5|Briefly described|p32|||See also P34. Early Cretaceous||||||
7072|Gearle Siltstone|31604|6|Mentioned|p6|||Cenomanian to Coniacian. Table 4.||||||
7072|Gearle Siltstone|32166|5|Briefly described|p159|||||||||
7072|Gearle Siltstone|32472|6|Mentioned|p10|||||||||
7072|Gearle Siltstone|32648|6|Mentioned|p32|||Winning Gp.||||||
7072|Gearle Siltstone|32711|6|Mentioned|Fig.3|||||||||
7072|Gearle Siltstone|32714|6|Mentioned|p84|||U.Cret. Winning Gp.||||||
7072|Gearle Siltstone|32715|6|Mentioned|Fig.16|||||||||
7072|Gearle Siltstone|32747|6|Mentioned|p365|||Sediments comparison||||||
7072|Gearle Siltstone|33015|6|Mentioned|p13|||||||||
7072|Gearle Siltstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
7072|Gearle Siltstone|33386|6|Mentioned|Fig.7|||||||||
7072|Gearle Siltstone|33450|6|Mentioned|Fig.5|||See P11.||||||
7072|Gearle Siltstone|33453|4|Described|p72|||||||||
7072|Gearle Siltstone|33835|6|Mentioned|p107|||||||||
7072|Gearle Siltstone|34112|6|Mentioned|p5|||Cenomanian - Lower Turonian||||||
7072|Gearle Siltstone|34363|6|Mentioned|p56|||Cenomanian. See also P57, Figs.7 & 8.||||||
7072|Gearle Siltstone|34702|6|Mentioned|p31|||||||||
7072|Gearle Siltstone|34727|6|Mentioned|p68|||||||||
7072|Gearle Siltstone|34838|6|Mentioned|p3|||||||||
7072|Gearle Siltstone|34846|6|Mentioned|Fig.3|||||||||
7072|Gearle Siltstone|35105|6|Mentioned|Fig.5|||||||||
7072|Gearle Siltstone|35144|6|Mentioned|p5|||||||||
7072|Gearle Siltstone|35282|6|Mentioned|Fig.19|||||||||
7072|Gearle Siltstone|35573|6|Mentioned|Fig.11|||Barrow-1 stratigraphic section||||||
7072|Gearle Siltstone|35972|6|Mentioned|p90|||||||||
7072|Gearle Siltstone|36093|6|Mentioned|Fig.2|||||||||
7072|Gearle Siltstone|36257|6|Mentioned|Table 2.1|||||||||
7072|Gearle Siltstone|36613|6|Mentioned|p1865|||||||||
7072|Gearle Siltstone|36890|3|Fully described|p297|||||||||
7072|Gearle Siltstone|37016|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7072|Gearle Siltstone|37306|6|Mentioned|p43|||||||||
7072|Gearle Siltstone|37320|6|Mentioned|p235|||||||||
7072|Gearle Siltstone|37360|4|Described|p575|||||||||
7072|Gearle Siltstone|37689|6|Mentioned|p23|||||||||
7072|Gearle Siltstone|38352|6|Mentioned|p61|||||||||
7072|Gearle Siltstone|38485|4|Described|p16|||||||||
7072|Gearle Siltstone|38486|6|Mentioned|p9|||||||||
7072|Gearle Siltstone|38655|6|Mentioned|p8|||||||||
7072|Gearle Siltstone|39158|5|Briefly described|p36|||||||||
7072|Gearle Siltstone|39211|6|Mentioned|p58|||Age||||||
7072|Gearle Siltstone|39427|4|Described|Table 1|||||||||
7072|Gearle Siltstone|39486|6|Mentioned|p2092|||||||||
7072|Gearle Siltstone|40340|6|Mentioned|p14|||||||||
7072|Gearle Siltstone|40342|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
7072|Gearle Siltstone|40343|5|Briefly described|p12|||||||||
7072|Gearle Siltstone|40617|6|Mentioned|p15|||||||||
7072|Gearle Siltstone|40800|6|Mentioned|p4|||||||||
7072|Gearle Siltstone|40801|6|Mentioned|p42|||||||||
7072|Gearle Siltstone|40877|5|Briefly described|p55|||||||||
7072|Gearle Siltstone|40992|6|Mentioned|Fig.8|||||||||
7072|Gearle Siltstone|41170|6|Mentioned|p155|||||||||
7072|Gearle Siltstone|41271|3|Fully described|p155|||||||||
7072|Gearle Siltstone|41280|6|Mentioned|p141|||||||||
7072|Gearle Siltstone|41436|6|Mentioned|p48|||||||||
7072|Gearle Siltstone|41438|6|Mentioned|p109|||||||||
7072|Gearle Siltstone|41440|4|Described|p139|||||||||
7072|Gearle Siltstone|41443|6|Mentioned|p164|||||||||
7072|Gearle Siltstone|41446|6|Mentioned|Fig.2|||||||||
7072|Gearle Siltstone|41447|6|Mentioned|Fig.3|||||||||
7072|Gearle Siltstone|41709|6|Mentioned|Fig.5|||||||||
7072|Gearle Siltstone|41712|6|Mentioned|Fig.8|||||||||
7072|Gearle Siltstone|42116|5|Briefly described|Fig.1 P6|||||||||
7072|Gearle Siltstone|42123|4|Described|p15|||||||||
7072|Gearle Siltstone|42463|6|Mentioned|Fig.2 P169|||||||||
7072|Gearle Siltstone|42598|5|Briefly described|P 95|||||||||
7072|Gearle Siltstone|42615|6|Mentioned|p6|||Triassic||||||
7072|Gearle Siltstone|42995|4|Described|p15|||see also Table 1.||||||
7072|Gearle Siltstone|43252|6|Mentioned|p163|||||||||
7072|Gearle Siltstone|43564|6|Mentioned|Fig.2,p446||Albian|||||||
7072|Gearle Siltstone|43598|6|Mentioned|p814|||||||||
7072|Gearle Siltstone|43712|5|Briefly described|p11||Aptian|||||||
7072|Gearle Siltstone|43722|6|Mentioned|p10-11|||||||||
7072|Gearle Siltstone|43826|6|Mentioned|Fig.2,p163|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
7072|Gearle Siltstone|43827|5|Briefly described|p193||Albian|Found at ODP sites 762,763||||||
7072|Gearle Siltstone|44235|14|Not recorded|p.120||Albian|||||||
7072|Gearle Siltstone|44344|14|Not recorded|p.18,20,24,opp.4,map|Turonian|Albian|Top fm of Winning Group. Albian-Turonian. (G50-1).||||||
7072|Gearle Siltstone|44345|14|Not recorded|map legend||Early Cretaceous|Lower Cretaceous.||||||
7072|Gearle Siltstone|44532|4|Described|p.9,16, map|||(G50-5).||||||
7072|Gearle Siltstone|44533|5|Briefly described|map legend||Early Cretaceous|Lower Cretaceous.||||||
7072|Gearle Siltstone|44537|14|Not recorded|map legend||Late Cretaceous|Upper Cretaceous.||||||
7072|Gearle Siltstone|44611|14|Not recorded|p20|||||||||
7072|Gearle Siltstone|44657|14|Not recorded|p.5,6,11,12,16|||||||||
7072|Gearle Siltstone|44998|14|Not recorded|p164|||Possibly correlates with Parda Formation.||||||
7072|Gearle Siltstone|45004|14|Not recorded|p.9|||||||||
7072|Gearle Siltstone|45015|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||31-MAY-06
7072|Gearle Siltstone|45142|6|Mentioned|Fig.4|||||||||
7072|Gearle Siltstone|48610|14|Not recorded|Pl.1,5,6|||||||||
7072|Gearle Siltstone|48628|14|Not recorded|p.4,5|||(F50-13/Wandagee).||||||
7072|Gearle Siltstone|48861|2|Defined|p.6-7|||p.1,5,9. Pl.1.||||||
7072|Gearle Siltstone|49942|4|Described|p4 Fig.3, p10|Late Cretaceous|Late Cretaceous|Unconformably overlain by Haycock Marl. Conformably overlies Windalia Radiolarite. Of Winning Group. Geological Province: Gascoyne Platform.||||||
7072|Gearle Siltstone|60118|6|Mentioned|p29|||Of the Winning Group. Geological Province: Barrow sub-basin.||||||
7072|Gearle Siltstone|60384|6|Mentioned|p243 Fig 2a, p261|Late Cretaceous|Late Cretaceous|Perth and Carnarvon Basins.||Of Winning Group.||||
7072|Gearle Siltstone|60725|6|Mentioned|p36 Fig.6. |Cretaceous|Cretaceous|||||||
7072|Gearle Siltstone|61555|5|Briefly described|p236|||Carnarvon Basin regional seals. Overlies Barrow Group.||||||02-FEB-10
7072|Gearle Siltstone|61811|5|Briefly described|p3 Fig.2, p9 Table 3, p13, p17.|Cenomanian|Cenomanian|Northern Perth Basin. Upper part of this unit is equivalent to upper Alinga Formation.||Unit in Winning Group.||Is overlain by Haycock Marl.|Discontinuous lenses of friable, dark grey silty mudstone with a thin (c.10 cm thick) fine-grained glauconitic sandstone layer at top.|
7072|Gearle Siltstone|61958|5|Briefly described|Map sheet 1|Early Cretaceous|Early Cretaceous|Of the Winning Group.||||||
7072|Gearle Siltstone|62734|5|Briefly described|p1362 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
7072|Gearle Siltstone|63068|5|Briefly described|p44 Fig. 2, p54, p56|Cenomanian|Albian|Of the Winning Group. Overlies Windalia Formation, or if absent, overlies Muderong Shale or Birdrong Sandstone. Geological Province: Carnarvon Basin. Coeval with Alinga Formation.||||||27-FEB-07
7072|Gearle Siltstone|64580|6|Mentioned|map legend|||Of Winning Group.||||||15-DEC-08
7072|Gearle Siltstone|64635|5|Briefly described|p4 Fig.3 |Cenomanian|Albian|||Unit in Winning Group.||||
7072|Gearle Siltstone|64973|5|Briefly described|p504, p504 Fig. 2, p505 Fig. 3|Albian|Albian|Of Winning Group. Geological Province: Carnarvon Basin. Also on p 509, p510.||||||
7072|Gearle Siltstone|64977|6|Mentioned|p493 Fig.3.|Late Cretaceous|Late Cretaceous|Thevenard Island area.||||Overlies Windalia Radiolarite. Is overlain unconformably by Toolonga Calcilutite.||
7072|Gearle Siltstone|64979|6|Mentioned|p548 Fig.17|||||||||
7072|Gearle Siltstone|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes dark grey friable mudstone.|
7072|Gearle Siltstone|67200|5|Briefly described|p8 fig 6, p17 table 1|Cretaceous|Cretaceous|Thermal conductivity of 1.23 W/mK. See also p49, p50, p53, app 2 p8. ||Winning Group||Overlies Windalia Radiolarite, unconformably overlain by Toolonga Calcilutite|Crudely bedded siltstone, friable mudstone.|
7072|Gearle Siltstone|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||Winning Group.||||
7072|Gearle Siltstone|67784|5|Briefly described|p26|Cenomanian|Albian|Carnarvon Basin. Up to 95m thick. Age range from diagnostic dinoflagellates, and calcareous and siliceous microfossils. See also references to Upper Gearle Siltstone (p26, p28 Tb.1, p32) and Lower Gearle Siltstone (p26, p28 Tb.1, p31, p32, p33).||||Overlies Windalia Radiolarite paraconformably.|Laminated pyritic mudstone and siltstone.|08-FEB-18
7072|Gearle Siltstone|67970|5|Briefly described|p4, p9, p10, p25 Fig.4.|Cenomanian|Albian|Exmouth Plateau.||Unit in Winning Group.||Overlies Windalia Radiolarite.|Shallow marine siltstone.|
7072|Gearle Siltstone|68206|6|Mentioned|p29-30|Albian|Albian|Carnarvon Basin. See also references to Gearle Siltstone, Lower (p30, 32) and Upper (p30, 32-33).||||Overlies Windalia Radiolarite.||
7072|Gearle Siltstone|69166|6|Mentioned|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|||Winning Group||||
7072|Gearle Siltstone|69182|5|Briefly described|Ch3 p8, Ch3 p12-p13|Cretaceous|Cretaceous|Carnarvon Basin. Split into an upper and lower part in Ch3 p17. See also Ch3 p17-p20, Ch3 p23-p26, Ch3 p35, Ch3 p37, Ch3 p50, Ch3 p52, Ch3 p53-p54, Ch3 p65-p66, Ch3 p69, Ch3 p71, Ch3 p73.||||Overlies the Windalia Radiolarite. Overlain by the Cape Range Group.|Glauconitic mudstone.|
7072|Gearle Siltstone|69185|5|Briefly described|500k_geologyp08_lut.csv|Cretaceous|Cretaceous|Of Northern Carnarvon Basin. Comprises northern part of the Winning Group.||Unit of Winning Group.||||
7072|Gearle Siltstone|69297|5|Briefly described|p247, p249|Aptian|Aptian|Gascoyne Sub-basin of the Southern Carnarvon Basin. Deposited in a shallow marine environment. ||Winning Group||Overlies the Windalia Radiolarite. Overlain by the Haycock Marl and the Toolonga Calcilutite.|Argillaceous siltstone.|
7072|Gearle Siltstone|69558|6|Mentioned|p258 Fig.419|Late Cretaceous|Early Cretaceous|||||Overlies Windalia Radiolarite.||
7072|Gearle Siltstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
7072|Gearle Siltstone|70066|5|Briefly described|Dampier: Fig.2; p3. Exmouth: Fig.2|Coniacian|Albian|See also Regional: Fig.6; p6-7, p16. Northern Carnarvon Basin. Oil reservoir in Barrow Sub-basin. Potential seal. Eroded during uplift in the early Santonian.||Winning Group.||Overlies Windalia Radiolarite. Is overlain by and intercalated with Haycock Marl.||
7072|Gearle Siltstone|70906|5|Briefly described|p757-758|Late Cretaceous|Early Cretaceous|Gorgon Platform. Doubly mis-spelt as Greale Slitstone on p757.||||Overlies Windalia Radiolarite. Is overlain by Toolonga Calcilutite.||
7072|Gearle Siltstone|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Plateau.||||Overlies Windalia Radiolarite. Is overlain by Toolonga Calcilutite.||
7073|Gearless Well trachyandesite|41741|6|Mentioned|p320|||Misspelling of Gearle?||||||
7085|Gee Cee Slate Member|30562|4|Described|p40|||See also P37||||||
7085|Gee Cee Slate Member|43162|6|Mentioned|6|||||||||
7187|Gidley Granophyre|23484|4|Described|p28|Archean|Archean|Intrudes the Fortescue Group.||||||07-NOV-08
7187|Gidley Granophyre|23570|3|Fully described|p159|Archean|Archean|Formerly referred to as "Dampier Granophyre".   Age: 2725+/-1.3Ma (U-Pb).   Geological Province: Pilbara Craton||||||07-NOV-08
7187|Gidley Granophyre|23575|5|Briefly described|Map Legend|||Geological Province Hamersley Basin.||||||
7187|Gidley Granophyre|23789|4|Described|p5 Fig. 3|Archean|Archean|Age: c.2725Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
7187|Gidley Granophyre|24169|5|Briefly described|p666 Fig. 5|||||||||
7187|Gidley Granophyre|24184|6|Mentioned|p712|Archean|Archean|Geological Province: Pilbara Craton. Age: ca.2725Ma. Intrudes the Dampier Granitoid Complex||||||07-NOV-08
7187|Gidley Granophyre|24192|5|Briefly described|p850|Archean|Archean|Geological Province: Hamersley Basin. Intrudes the Fortescue Group||||||07-NOV-08
7187|Gidley Granophyre|24391|5|Briefly described|p8-3|Archean|Archean|Age: 2725 Ma. Intrudes Dampier Granitoid subcomplex. Geological Province: Pilbara Block.||||||07-NOV-08
7187|Gidley Granophyre|24541|3|Fully described|p12-13, p53-56|Paleoproterozoic|Neoarchean|Age: 2725+/-3 Ma. Geological Province: Pilbara Craton. Total thickness: 2km. Intrudes along the basal unconformity of the Fortescue Group.||||||07-NOV-08
7187|Gidley Granophyre|24543|5|Briefly described|Map legend|Archean|Archean|||||||23-DEC-09
7187|Gidley Granophyre|30490|2|Defined|p108|Precambrian|Precambrian|See also p109-113.||||||21-AUG-07
7187|Gidley Granophyre|30766|6|Mentioned|Fig.1|||||||||
7187|Gidley Granophyre|32532|6|Mentioned|p817|||Re dates||||||
7187|Gidley Granophyre|33542|6|Mentioned|p412|||||||||
7187|Gidley Granophyre|35260|5|Briefly described|Table 1|||||||||
7187|Gidley Granophyre|36882|4|Described|p137|||||||||
7187|Gidley Granophyre|37460|6|Mentioned|p113|||||||||
7187|Gidley Granophyre|39697|4|Described|p133|||See also PP22,52||||||
7187|Gidley Granophyre|43652|6|Mentioned|p390|||||||||
7187|Gidley Granophyre|43822|5|Briefly described|map legend|Archean|Archean|||||||07-NOV-08
7187|Gidley Granophyre|44152|4|Described|p174-175|||Kriewaldt (1964); de Laeter and Trendall (1971). Intruded along the basal unconformity of the Fortescue Group in Dampier Archipelago area. Rb-Sr whole-rock isochron age; not definitive.|2196 +/- 26 Ma (de Laeter and Trendall, 1971).|||Intrudes Fortescue Group.|Thick sheet of massive, dark-green, dark-blue, purple or black granophyre with basal gabbro.|
7187|Gidley Granophyre|50382|5|Briefly described|Map Legend|Archean|Archean|Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
7187|Gidley Granophyre|60373|6|Mentioned|p146 Fig. 1|||||||||
7187|Gidley Granophyre|63441|5|Briefly described|p37|Archean|Archean|Age: 2725Ma. Intrudes the Hearson Monzogranite outcrops along the Burrup Peninsula and Dampier Archipelago islands.||||||07-FEB-11
7187|Gidley Granophyre|64174|5|Briefly described|Map legend|Archean|Archean|Of the Flying Foam Suite.  Age: c.2724Ma.||||||07-NOV-08
7187|Gidley Granophyre|64580|4|Described|map legend||Neoarchean|Of Flying Foam Suite. Fine- to medium-grained granophyre; commonly porphyritic.||||||09-DEC-08
7187|Gidley Granophyre|67201|4|Described|p16-17 Fig.9, p29 Fig.15|Archean|Archean|Pilbara Craton. Northern Fortescue Basin, Northwest Pilbara Sub-basins. In Roebourne-Karratha area.||Flying Foam Suite|||Fine- to medium-grained granophyre; commonly pophyritic.|
7187|Gidley Granophyre|67229|6|Mentioned|p2 Fig.1|||Fortescue Basin.||||||
7187|Gidley Granophyre|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. [Stated to be part of Fortescue Group on 500k_interpgeop_pilcrat02_lut.csv]. Likely to be an intrusive unit intruding into Fortescue Group. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv, 500k_interpgeol_pilcrat02_lut.csv.|c. 2725 Ma|Unit of Flying Foam Suite.|||Fine- to medium-grained granophyre; commonly porphyritic, gabbro.|
7187|Gidley Granophyre|69301|6|Mentioned|p18 Fig.7|||Pilbara Craton. Fortescue Basin. Northwest Pilbara Sub-basin, Sequence 3.||||||
7187|Gidley Granophyre|70775|5|Briefly described|p15|||Pilbara Craton.||Flying Foam Suite|||Fine- to medium-grained granophyre; commonly porphyritic gabbro.|
7187|Gidley Granophyre|70826|6|Mentioned|p8|Neoarchean|Neoarchean|Intrudes the western Pilbara Craton.||Flying Foam Suite||||
7187|Gidley Granophyre|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granophyre, gabbro|
7187|Gidley Granophyre|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Northwest Pilbara Sub-basin, Fortescue Basin. Shown with an informal unnamed member.|2725+/-3 Ma|Flying Foam Suite|||Fine- to medium-grained granophyre; commonly porphyritic; underlain by gabbro. Gabbro; locally with large pyroxene crystals.|
7206|Giles Complex|22445|5|Briefly described|p16||Stenian|Musgrave Block||||||
7206|Giles Complex|22635|6|Mentioned|p492||Stenian|||||||
7206|Giles Complex|22716|5|Briefly described|table4, p238|Stenian|Stenian|Age: 1080 Ma||||||
7206|Giles Complex|22804|6|Mentioned|p442|||Age - 1100-1200 Ma.||||||
7206|Giles Complex|23400|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
7206|Giles Complex|23483|5|Briefly described|p4|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|23716|5|Briefly described|p4|||See also page 6 Table 1, also page 18.||||||
7206|Giles Complex|23818|6|Mentioned|p39|||Geological Province: Musgrave Block.||||||
7206|Giles Complex|23892|5|Briefly described|p42 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
7206|Giles Complex|24115|5|Briefly described|p31 Fig.28|Mesoproterozoic|Mesoproterozoic|Age: 1078+/-5 Ma (U-Pb)||||||
7206|Giles Complex|24168|6|Mentioned|p639|Mesoproterozoic|Mesoproterozoic|Age: ca 1080Ma||||||03-AUG-09
7206|Giles Complex|24169|6|Mentioned|p674|||||||||
7206|Giles Complex|24197|5|Briefly described|p97|||Overlain by Bentley Supergroup.||||||07-FEB-11
7206|Giles Complex|24301|6|Mentioned|p29|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block||||||
7206|Giles Complex|24442|5|Briefly described|p28 Fig.1|Mesoproterozoic|Mesoproterozoic|Age: 1080Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Age: ~1080 Ma. Over 20 massive and layered mafic-ultramafic intrusive bodies. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|24499|5|Briefly described|Map legend|||||||||
7206|Giles Complex|24522|5|Briefly described|p80 Fig. 2|||Age: 1078Ma (Glikson et al 1996). Geological Province: Musgrave Block (Centralian Superbasin). See also p81 Fig. 3, p85-86.||||||03-AUG-09
7206|Giles Complex|24535|5|Briefly described|p16, p19 Fig.15|Mesoproterozoic|Mesoproterozoic|Of Musgrave Complex. U-Pb ages  ~1075 Ma for mafic intrusives rocks of this complex.||||||26-NOV-13
7206|Giles Complex|30202|6|Mentioned|p146|||||||||
7206|Giles Complex|30385|6|Mentioned|Table 1|||||||||
7206|Giles Complex|30386|4|Described|p13|||||||||
7206|Giles Complex|30388|6|Mentioned|p20|||On Table 1 P20||||||
7206|Giles Complex|30389|4|Described|p8|||Middle Proterozoic||||||
7206|Giles Complex|30390|4|Described|p100|||See also p101-193.||||||19-SEP-06
7206|Giles Complex|30391|5|Briefly described|p455|||||||||
7206|Giles Complex|30399|6|Mentioned|p657|||||||||
7206|Giles Complex|30513|6|Mentioned|p44|||||||||
7206|Giles Complex|30602|6|Mentioned|p658|||||||||
7206|Giles Complex|30703|6|Mentioned|p76|||Magnetic properties||||||
7206|Giles Complex|30704|4|Described|p45|||Precambrian age. See also p46-61.||||||19-SEP-06
7206|Giles Complex|30705|6|Mentioned|p517|||Precambrian age. See also P518-520||||||
7206|Giles Complex|30706|4|Described|p51|||Precambrian layered intrusions. See also p52-58.||||||19-SEP-06
7206|Giles Complex|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
7206|Giles Complex|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
7206|Giles Complex|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30943|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|31069|6|Mentioned|p187|||Refers Nesbitt et al. (1970)||||||
7206|Giles Complex|31070|6|Mentioned|p546|||||||||
7206|Giles Complex|31071|6|Mentioned|p375|||||||||
7206|Giles Complex|31072|5|Briefly described|p77|||See also p78, 79||||||19-SEP-06
7206|Giles Complex|31323|5|Briefly described|p1009|||||||||
7206|Giles Complex|31393|6|Mentioned|Pl.25|||||||||
7206|Giles Complex|31923|6|Mentioned|p6|||||||||
7206|Giles Complex|31970|4|Described|p13|||?Equivalents described||||||
7206|Giles Complex|32147|5|Briefly described|p165|||||||||
7206|Giles Complex|32192|4|Described|p158|||1000-1100my||||||
7206|Giles Complex|32280|4|Described|p115|||Mineralogy. See also p116-125.||||||19-SEP-06
7206|Giles Complex|32548|6|Mentioned|p71|||||||||
7206|Giles Complex|32692|6|Mentioned|p186|||Olivine cell dimensions||||||
7206|Giles Complex|32694|6|Mentioned|p1109|||||||||
7206|Giles Complex|33244|6|Mentioned|p1009|||||||||
7206|Giles Complex|33468|6|Mentioned|Fig.7|||||||||
7206|Giles Complex|33478|6|Mentioned|p451|||||||||
7206|Giles Complex|34208|6|Mentioned|p280|||||||||
7206|Giles Complex|34287|6|Mentioned|p32|||||||||
7206|Giles Complex|34364|6|Mentioned|Fig.1|||||||||
7206|Giles Complex|34537|6|Mentioned|p39|||||||||
7206|Giles Complex|34604|6|Mentioned|p254|||Age.||||||
7206|Giles Complex|34608|6|Mentioned|p4|||Middle Proterozoic||||||
7206|Giles Complex|34685|6|Mentioned|p353|||||||||
7206|Giles Complex|34688|6|Mentioned|p341|||||||||
7206|Giles Complex|34689|6|Mentioned|p137|||||||||
7206|Giles Complex|34718|6|Mentioned|p12|||||||||
7206|Giles Complex|34834|6|Mentioned|p221|||||||||
7206|Giles Complex|34995|6|Mentioned|p79|||||||||
7206|Giles Complex|35308|6|Mentioned|p451|||||||||
7206|Giles Complex|35323|4|Described|p404|||||||||
7206|Giles Complex|35468|6|Mentioned|p21|||||||||
7206|Giles Complex|35469|6|Mentioned|p46|||Also shown on Fig.9||||||
7206|Giles Complex|35495|6|Mentioned|p341|||||||||
7206|Giles Complex|35628|6|Mentioned|p10|||||||||
7206|Giles Complex|35726|6|Mentioned|p102|||||||||
7206|Giles Complex|36308|6|Mentioned|p211|||||||||
7206|Giles Complex|36458|6|Mentioned|p471|||||||||
7206|Giles Complex|36551|6|Mentioned|p115|||See also P24.||||||
7206|Giles Complex|36701|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|36886|3|Fully described|p201|||||||||
7206|Giles Complex|36964|6|Mentioned|p247|||||||||
7206|Giles Complex|37697|6|Mentioned|p189|||||||||
7206|Giles Complex|37707|6|Mentioned|p25|||||||||
7206|Giles Complex|37818|6|Mentioned|p77|||||||||
7206|Giles Complex|38490|6|Mentioned|p308|||||||||
7206|Giles Complex|38761|6|Mentioned|p41|||||||||
7206|Giles Complex|38995|6|Mentioned|p9|||||||||
7206|Giles Complex|39888|6|Mentioned|p464|||See also pP475.||||||19-SEP-06
7206|Giles Complex|40229|6|Mentioned|p24|||||||||
7206|Giles Complex|40309|6|Mentioned|p90|||||||||
7206|Giles Complex|40583|6|Mentioned|p449|||||||||
7206|Giles Complex|41074|4|Described|p174|||||||||
7206|Giles Complex|41594|5|Briefly described|p72|||Also mention p30.||||||19-SEP-06
7206|Giles Complex|41638|6|Mentioned|p6|||||||||
7206|Giles Complex|41640|5|Briefly described|p9|||||||||
7206|Giles Complex|41957|6|Mentioned|p66|||||||||
7206|Giles Complex|42325|4|Described|p6-7|||||||||
7206|Giles Complex|42330|4|Described|p1443|||||||||
7206|Giles Complex|42337|4|Described|p2|||||||||
7206|Giles Complex|42775|5|Briefly described|Fig.13 P323|||||||||
7206|Giles Complex|42794|6|Mentioned|p3|||||||||
7206|Giles Complex|42940|6|Mentioned|p1|||||||||
7206|Giles Complex|43052|4|Described|p160|||Age of 1200 - 1185 Ma||||||
7206|Giles Complex|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Basic to ultrabasic intrusive complex.||||||26-MAY-05
7206|Giles Complex|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7206|Giles Complex|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
7206|Giles Complex|43561|5|Briefly described|Fig.3,1434,1436,1438|||||||||
7206|Giles Complex|43591|6|Mentioned|p193|||||||||
7206|Giles Complex|43609|2|Defined|p13|Stenian|Stenian|SHRIMP U/Pb ages 1052 - 1078 Ma||||||11-SEP-08
7206|Giles Complex|43644|6|Mentioned|p592|||||||||
7206|Giles Complex|43688|5|Briefly described|p174|||||||||
7206|Giles Complex|43691|5|Briefly described|p147|||||||||
7206|Giles Complex|43692|5|Briefly described|p127||Proterozoic|||||||
7206|Giles Complex|43693|5|Briefly described|p107|||||||||
7206|Giles Complex|43694|5|Briefly described|p91|||||||||
7206|Giles Complex|43695|5|Briefly described|p69||Neoproterozoic|||||||
7206|Giles Complex|43696|5|Briefly described|p41|||||||||
7206|Giles Complex|43728|3|Fully described|p1-73|Neoproterozoic|Mesoproterozoic|||||||
7206|Giles Complex|43806|6|Mentioned|p365|||||||||
7206|Giles Complex|43969|14|Not recorded|Map Legend|||||||||
7206|Giles Complex|43971|14|Not recorded|p54||Archean|||||||07-NOV-08
7206|Giles Complex|44109|4|Described|p1|Mesoproterozoic|Mesoproterozoic|Consists of massive, partly deformed and recrystallised, layered mafic-ultramafic intrusions emplaced in the southern granulite-facies zone of   Musgrave Block.  Age: 1078+/-3Ma. ||||||
7206|Giles Complex|44139|6|Mentioned|p283-286|||Comprises several isolated sheet-like bodies of layered-basic plutonic rocks. Includes (in WA) Jameson Range, Blackstone Range, Michael Hills and Hinckley Range Gabbros. Intrudes Bentley Supergroup.| | ||||05-MAR-18
7206|Giles Complex|45087|5|Briefly described|p210|||See also p211. Chem. analyses.||||||19-SEP-06
7206|Giles Complex|45139|14|Not recorded|?|||||||||
7206|Giles Complex|45149|6|Mentioned|p19|||||||||
7206|Giles Complex|47055|5|Briefly described|p513|||||||||
7206|Giles Complex|49833|5|Briefly described|p7|||||||||
7206|Giles Complex|50607|6|Mentioned|p1.1|||Geological Province: Musgrave Block.||||||
7206|Giles Complex|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite.  Age: ~1078Ma.||||||
7206|Giles Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Generally mafic. Geological Province: Musgrave Block.||||||22-FEB-05
7206|Giles Complex|60662|5|Briefly described|Map legend|||Variably magnetic mafic-ultramafic intrusives.||||||22-FEB-05
7206|Giles Complex|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Occurred during the Giles Event from 1080-1040Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Geological Province: Musgrave Block.||||||
7206|Giles Complex|60683|4|Described|p19, p10 Tb. 1|Mesoproterozoic|Mesoproterozoic|Extensive suite of massive layered mafic to ultramafic intrusions; pyroxenite and norite. Age: 1078+/-3Ma (Sun et al 1996). In NT and SA within the Musgrave Block.||||||03-AUG-09
7206|Giles Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1078Ma. Basic to ultrabasic layered intrusive complex.||||||
7206|Giles Complex|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Basic to ultrabasic layered intrusive complex. Age: 1078 Ma.||||||
7206|Giles Complex|61154|4|Described|p13, p15|Mesoproterozoic|Mesoproterozoic|Extensive suite of massive layered maific to ultramafic intrusions, emplaced within the granulite facies terrane of the central to western Musgrave Block. Age: 1080-1040Ma. Geological Province: Musgrave Block. See also p3, p31.||||||
7206|Giles Complex|61339|6|Mentioned|Map legend|||See also in Solid Geology Sketch Map.||||||21-SEP-05
7206|Giles Complex|61340|6|Mentioned|Summary chart/Map legend|||Age: ~1080Ma.||||||
7206|Giles Complex|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Pyroxenite and norite. Age: ~1078Ma. Geological Province: Musgrave Block.||||||03-AUG-09
7206|Giles Complex|61524|5|Briefly described|p16|||Large, layered mafic-ultramafic intrusives. Age: 1080 Ma. Geological Province: Musgrave Province.||||||
7206|Giles Complex|61733|5|Briefly described|p45-46|||Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|||||Layered mafic intrusive bodies.|
7206|Giles Complex|61864|4|Described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Also part of Warrakurna large igneous province. Main focus for Ni-Cu mineralisation. More detail of metamorphism on p18.|~1080 Ma||||Extensive voluminous mafic/ultramafic sequence (vertically stacked magma chambers with associated feeder dykes).|
7206|Giles Complex|62428|5|Briefly described|p351 Tb. 6|||Age: 1078+/-5Ma (SHRIMP U-Pb). Palaeomagnetic data.||||||10-FEB-09
7206|Giles Complex|62989|6|Mentioned|p39|||Rocks are geochemically similar to Mount Harris Basalt.||||||25-JAN-07
7206|Giles Complex|63224|6|Mentioned|p9|Neoproterozoic|Neoproterozoic|||||||02-MAY-07
7206|Giles Complex|63465|5|Briefly described|p551, p554|||Consists of a series of partly deformed and recrystallised layered mafic-ultramafic intrusions, mafic and felsic dykes, coeval mafic and felsic volcanic rocks; includes recrystallised gabbro troctolitic, gabbroic and ultramafic intrusions. Musgrave Block||||||03-AUG-09
7206|Giles Complex|64645|5|Briefly described|p16, p16 Fig. 2, p17, p18, p19|Mesoproterozoic|Mesoproterozoic|Age: 1080Ma. Geological Province: Musgrave Province. Mafic - ultramafic rocks.||||||
7206|Giles Complex|64722|5|Briefly described|Fig. 2 p3-6, p17, 22|Stenian|Stenian|Musgrave Inlier. U-Pb zircon age determined from a leucogranite interpreted as part of the intrusion.|1078 +/- 3 Ma.||||Mafic-ultramafic layered intrusions.|11-APR-12
7206|Giles Complex|64745|5|Briefly described|p376, p377, p370, p371, p373 Fig. 3|Stenian|Stenian|Mafic-ultramafic; layered intrusions are generally fault bound; Ni-PGE prospective. Age: 1.08 Ga. Geol. Prov: Fregon Domain, Musgrave Province. See also Giles Intrusions. Geol. Prov: Warakurna Large Igneous Province.||||||18-SEP-09
7206|Giles Complex|64831|5|Briefly described|p1128 Figs. 1, 2|||Layered mafic and ultramafic intrusions. See also pages 1130,1133.||||||
7206|Giles Complex|65256|6|Mentioned|p4-5, p21, p27, p31|Stenian|Stenian|Western Musgrave Block. Layered mafics to ultramafics, emplaced deeply into continental crust. 1078 Ma; coeval with Alcurra dolerite.||||||
7206|Giles Complex|65309|6|Mentioned|p5 Fig.6. |||||||||
7206|Giles Complex|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Mafic to ultramafic intrusive rocks.|
7206|Giles Complex|65385|6|Mentioned|pS131 Tab.2|Stenian|Stenian|1080-1040 Ma.||||||08-MAR-12
7206|Giles Complex|65693|6|Mentioned|p3.|Mesoproterozoic|Mesoproterozoic|Term used (Daniels 1974) to refer to Warakurna Supersuite or Giles Event.||||||
7206|Giles Complex|65906|6|Mentioned|p3, p6, p7|Mesoproterozoic|Mesoproterozoic|Mafic and ultramafic layered intrusions. Folded and subsequently cut by 1075 +/- 7 Ma Giles Event granite dykes. Is part of Warakurna Supersuite. Is overlain by Tollu Group.||||||
7206|Giles Complex|66256|6|Mentioned|p17 Fig.13|||Musgrave Province.||||||
7206|Giles Complex|66526|5|Briefly described|p15, p24.|||Mafic and ultramafic intrusions in the Musgrave Province of the Warakurna Large Igneous Province. Significant for their size and mineralisation. Age of a (?) sill associated with Bell Rock intrusion.|1078 +/- 3 Ma minimum.|||||
7206|Giles Complex|67128|5|Briefly described|p5 Fig.4|||Warakurna Large Igneous Province. Also (and in this Report, more commonly) called Giles intrusions (p6-7, p10-11, p15, p18-21). At least 20 sheet-like bodies across the Musgrave Province; described in some detail. Forms ranges with parallel ridges that correspond to aeromagnetic and gravity highs.|||||Ultramafic, gabbroic and troctolitic layered intrusions.|
7206|Giles Complex|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|~1080-1040 Ma.|||||
7206|Giles Complex|67462|5|Briefly described|Map legend.|||||||||
7206|Giles Complex|67536|5|Briefly described|Map Legend|Stenian|Stenian|Coompana Block. Informally subdivided into three parts. Rocks mapped as equivalent to the Giles Complex have an age of ca. 1078 - 1073 Ma ? These comprise gabbro and reversely magnetised bodies, possibly mafic or ultramafic.|ca. 1078 - 1073 Ma ?||||Massive anorthosite; non-magnetic to weakly magnetic; layered ultramafic and mafic sills with contrasting magnetic character; massive to weakly layered mafic to ultramafic rocks, commonly basal to layered sills; non-magnetic to weakly magnetic.|
7206|Giles Complex|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Mafic to ultramafic intrusive rocks.|
7206|Giles Complex|69003|5|Briefly described|p48 Fig.57, p51, p74|Mesoproterozoic|Mesoproterozoic|Cogenetic with the c.1068 Ma Nebo-Babel intrusion which hosts the world-class magmatic Ni-Cu-PGE sulfide deposit. A gabbroic intrusive is related to the Tollu Cu-Co prospect. Also included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|1078 Ma.|Warakurna Supersuite.||||
7206|Giles Complex|69091|6|Mentioned|p117 Fig.5.15, p142, p203|||See Giles Suite.|||||Ultramafics.|26-SEP-14
7206|Giles Complex|69153|6|Mentioned|Rocks.csv|||Sample descriptions|||||Norite, including coarse-grained norite; gabbronorite, including coarse-grained olivine gabbronorite; dunite; dolerite; olivine orthopyroxenite; lherzolite; pyroxene peridotite|
7206|Giles Complex|69436|5|Briefly described|p21:1, 10-12, 21|Mesoproterozoic|Mesoproterozoic|Central and western Musgrave Province. An extensive suite of massive, layered mafic to ultramafic intrusions emplaced within granulite-facies terranes. A single outcrop occurs in NT, SW of the Mann Ranges on a hill at the SA border; has more significant subsurface extent. Supergene enrichment of lateritised rocks of this unit in SA has produced Ni accumulations very close to the NT border. Hosts the Nebo-Babel Ni-Cu(-PGE) deposit in WA. Geochronology by Sun et al. (1996) and Howard et al. (2011) respectively.|1078 +/- 3 Ma and 1076 +/- 4 Ma.|Warakurna Supersuite.|||A medium- to coarse-grained pyroxenite with minor gabbro. Contains pseudotachylite, but no pervasive fabric. Locally capped by calcrete, laterite, chalcedony and pale brown jasper.|12-JUL-16
7206|Giles Complex|69437|5|Briefly described|p22:11|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the granulite-facies terrane of the C-W Musgrave Province.|||||Layered mafic and ultramafic intrusions.|12-JUL-16
7206|Giles Complex|69640|6|Mentioned|p174|||||||||
7206|Giles Complex|69648|6|Mentioned|p11|||Giles Complex and Tollu Volcanics, of western Musgrave Block (Fanning 1997 and Fanning et al. 2007), are compared to mafic magmatism in Proterozoic rocks in undifferentiated basement underlying Officer Basin.||||||
7206|Giles Complex|69926|6|Mentioned|p157|||Musgrave Block.|||||Layered ultramafic igneous complex.|
7206|Giles Complex|69937|5|Briefly described|p16, p34|||One of the possible sediment sources for the Amadeus Basin.|1090-1040 Ma.|||||
7206|Giles Complex|70083|6|Mentioned|p206-207|||Musgrave Inlier.|1085-1040 Ma.||Alcurra Dolerite.||Mafic and ultramafic rocks.|
7206|Giles Complex|70316|6|Mentioned|p120|||Warakurna LIP.|1073 +/- 5 Ma; 1058 +/- 14 Ma.|||||
7206|Giles Complex|71321|5|Briefly described|p5,11,22,54,64,66-67|Stenian|Stenian|Geological province: Musgrave Province. Variably deformed mafic-ultramafic layered intrusions associated with c. 1085-1040 Ma Giles Event (p11 for references). Considered to be prospective for Ni, Cu, Co, Cr, PGE, V and Ti. Sample of amphibolite facies meta-ultramafic rock (partly mylonitised hornblende-orthopyroxene-olivine-phlogopite-magnetite) of possible cumulate nature recovered from drillhole TIE RC 80 from 6-36m interval (Tucker et al., 2012) which may belong to Giles Complex. This sample was likely deformed and mylonitised during Neoproterozoic-Cambrian Petermann Orogeny. This sample is only known in this drillhole, and does not crop out in the study area. See p54 for geochmical breakdown of the ultramafic intrusion suspected to be of Giles Complex.|1085-1040 Ma|||||
7206|Giles Complex|71322|5|Briefly described|p11, p26, p28|||Summary log for drillhole DD10WOD007.|||||Anorthosite, leucogabbro, leucogabbronorite, gabbro, gabbronorite, olivine gabbro, troctolite, pyroxenite.|
7206|Giles Complex|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||~1080 Ma.|||Correlated with Alcurra Dolerite.||
7206|Giles Complex|71536|6|Mentioned|p69, p78||||c. 1080 Ma|||||
7206|Giles Complex|72238|5|Briefly described|p34, 35|Stenian|Stenian|Mafic-ultramafic intrusions that are prospective for orthomagmatic Ni-Cu - platinum group elements (PGE) mineralisation (Howard et al. 2009). Associated with coeval Alcurra Dolerite.||||||17-SEP-19
7206|Giles Complex|72476|6|Mentioned|p25 Fig.2|||Musgrave Province.||||||
7206|Giles Complex|72934|6|Mentioned|p12|||Musgrave Province. Part of the Warakurna large igneous province/Ngaanyatjarra Rift[?].||||||
7206|Giles Complex|73225|5|Briefly described|p5|||Warakurna Large Igneous Province.|c.1074 Ma.|||Correlated with Giants Head and Warbla Suites (Warakurna Supersuite).||
7206|Giles Complex|73232|6|Mentioned|p5|Stenian|Stenian|Musgrave Province. [Emplaced] during the Giles Event.|c. 1085-1030 Ma||Alcurra Dolerite|Intrudes Birksgate Complex and Pitjantjatjara Supersuite.|Includes mafic rocks.|
7247|Gindalbie Group|37373|5|Briefly described|Table 2.I|||||||||
7247|Gindalbie Group|39869|6|Mentioned|Fig.2|||||||||
7247|Gindalbie Group|41249|5|Briefly described|Table 1|||||||||
7247|Gindalbie Group|43075|5|Briefly described|Table 1|||||||||
7247|Gindalbie Group|46416|6|Mentioned|p2|||||||||
7247|Gindalbie Group|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2697 - 2671 Ma (inferred).||Includes Little Peters Formation, Kents Bore Basalt||Mylonitized psammite and pelite. Komatiitic basalt and minor dolerite schist.|
7247|Gindalbie Group|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). Tectonically juxtaposed against Marshall Pool Subgroup along the Ockerburry and Perseverance Faults.|2694-2676 Ma (inferred)||Includes Kents Bore Basalt, Little Peters Formation, Melita Formation, Teutonic Bore Formation.||Komatiitic basalt and minor mafic schist; mylonitised psammite and pelite.|
7247|Gindalbie Group|72095|6|Mentioned|p3 Fig 2, p5 Fig 3|||Kurnalpi Terrane, Eastern Goldfields, Yilgarn Craton.||||||
7247|Gindalbie Group|72491|6|Mentioned|p5 Fig.4|||Kurnalpi Terrane, Yilgarn Craton.||||||
7247|Gindalbie Group|73596|6|Mentioned|p1162-1163|||Leonora-Windarra Inlier, Kalgoorlie Terrane.||||Overlies Mount Fouracre Basalt (Marshall Pool Subgroup). Is overlain by Pig Well Formation.|Felsic volcanic and associated volcanoclastic rocks.|
7259|Gingin Chalk|12758|5|Briefly described|p22, p3 Fig. 3|Cretaceous|Cretaceous|Of the Coolyena Group.||||||
7259|Gingin Chalk|12759|3|Fully described|p42; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Campanian|Santonian|Defined Glauert (1910); Type section in MacIntyre Gully, 1.6km N of Gingin, (AMG Z50, 395333 m E, 6534769 m N). Max thickness is 40m.||Of Coolyena Group.||Overlies the Molecap Greensand (conformably) and Leederville and Osborne Formations (unconformably). Overlain conformably by the Poison Hill Greensand.|Weakly to moderately consolidated, pale grey to whitish-green, slightly glauconitic chalk with sandy beds.|12-MAY-14
7259|Gingin Chalk|14227|5|Briefly described|p9. Enclos. 2|Maastrichtian|Campanian|Carbonate sediments. Presented as Gingin only in Enclosure 2.||||||07-FEB-11
7259|Gingin Chalk|23279|6|Mentioned|p31|||||||||
7259|Gingin Chalk|23815|5|Briefly described|p298|Santonian|Santonian|Geological Province: Perth Basin.||||||18-APR-05
7259|Gingin Chalk|23816|4|Described|p250, 251|Campanian|Santonian|Geological Province: Perth Basin. Of the Coolyena Group. Disconformably underlain by Dandaragan Sandstone, or conformably by Molecap Greensand. Conformably overlain by Poison Hill Greensands. Max thickness: 19 m. Richly fossiliferous.||||||22-JUL-09
7259|Gingin Chalk|24058|5|Briefly described|p111 Fig. 4|Cretaceous|Cretaceous|Geological Basin: Perth Basin.||||||
7259|Gingin Chalk|24094|5|Briefly described|p268, p275|Campanian|Santonian|Overlies Poison Hill Greensand. See also Gingin Chalk formation. Geological Province: Perth Basin.||||||22-JUL-09
7259|Gingin Chalk|24160|6|Mentioned|p95 Tb.57.|Late Cretaceous|Late Cretaceous|||||Overlies Molecap Greensand. Is overlain by Poison Hill Greensand.||
7259|Gingin Chalk|24351|6|Mentioned|p16|||Geological Province: Perth Basin.||||||13-DEC-07
7259|Gingin Chalk|24551|6|Mentioned|p632|||||||||
7259|Gingin Chalk|29382|6|Mentioned|Table 10|||||||||
7259|Gingin Chalk|29693|6|Mentioned|Fig.7|||||||||
7259|Gingin Chalk|29721|6|Mentioned|Table 226|||||||||
7259|Gingin Chalk|30188|2|Defined|p75|Late Cretaceous|Late Cretaceous|See also p75. Refers Glauert (1910).||||||04-SEP-14
7259|Gingin Chalk|31153|6|Mentioned|Fig. 57|||Refers Cockbain & Playford (1973)||||||
7259|Gingin Chalk|31238|6|Mentioned|p27|||See also Fig. 12A||||||
7259|Gingin Chalk|31562|6|Mentioned|p11|||||||||
7259|Gingin Chalk|31568|5|Briefly described|p19|||U. Cretaceous||||||
7259|Gingin Chalk|32391|6|Mentioned|p1|||||||||
7259|Gingin Chalk|32648|6|Mentioned|p32|||Santonian||||||
7259|Gingin Chalk|32714|6|Mentioned|Fig.2|||||||||
7259|Gingin Chalk|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
7259|Gingin Chalk|33044|4|Described|p44|||See also diagrams 16 & 21||||||
7259|Gingin Chalk|33165|6|Mentioned|Chart|||Correlation chart only||||||
7259|Gingin Chalk|33386|6|Mentioned|Fig.7|||||||||
7259|Gingin Chalk|34413|6|Mentioned|p13|||Senonian||||||
7259|Gingin Chalk|34414|6|Mentioned|p53|||Senonian||||||
7259|Gingin Chalk|34841|6|Mentioned|Fig.2|||||||||
7259|Gingin Chalk|34951|6|Mentioned|p111|||||||||
7259|Gingin Chalk|35026|6|Mentioned|p331|||||||||
7259|Gingin Chalk|35057|6|Mentioned|p301|||||||||
7259|Gingin Chalk|35059|6|Mentioned|Table.19|||||||||
7259|Gingin Chalk|35100|6|Mentioned|p165|||||||||
7259|Gingin Chalk|35282|6|Mentioned|Fig.2|||See also P30.||||||
7259|Gingin Chalk|35638|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
7259|Gingin Chalk|35697|6|Mentioned|p91|||||||||
7259|Gingin Chalk|35968|5|Briefly described|p64|||See also Table 4.||||||
7259|Gingin Chalk|35970|6|Mentioned|Table 12|||||||||
7259|Gingin Chalk|35973|5|Briefly described|p94|||||||||
7259|Gingin Chalk|36257|6|Mentioned|Table 2.1|||||||||
7259|Gingin Chalk|36265|5|Briefly described|Fig.3.26|Late Cretaceous|Late Cretaceous|Of the Coolyena Group. Geological province: Perth Basin.||||||04-MAR-08
7259|Gingin Chalk|36293|2|Defined|p184|Campanian|Santonian|Santonian-Campanian.||||||
7259|Gingin Chalk|36305|6|Mentioned|p352|||||||||
7259|Gingin Chalk|36890|3|Fully described|p250|||||||||
7259|Gingin Chalk|37104|6|Mentioned|Fig.3|||||||||
7259|Gingin Chalk|37344|6|Mentioned|p76|||||||||
7259|Gingin Chalk|37360|6|Mentioned|Fig.3|||||||||
7259|Gingin Chalk|37577|6|Mentioned|p75|||||||||
7259|Gingin Chalk|39923|6|Mentioned|p354|||||||||
7259|Gingin Chalk|40348|6|Mentioned|Map legend|Santonian|Santonian|||||||
7259|Gingin Chalk|40349|5|Briefly described|p17|||||||||
7259|Gingin Chalk|41422|6|Mentioned|p163|||||||||
7259|Gingin Chalk|42123|4|Described|p19|||||||||
7259|Gingin Chalk|42393|5|Briefly described|p101|||Perth Basin||||||
7259|Gingin Chalk|42473|6|Mentioned|p64|||||||||
7259|Gingin Chalk|42995|4|Described|p19|||see also Table 1.||||||
7259|Gingin Chalk|43347|6|Mentioned|9|||||||||
7259|Gingin Chalk|43700|6|Mentioned|Fig.2,p21||Cretaceous|||||||
7259|Gingin Chalk|44144|4|Described|p503 Tb.4-21, p517|Campanian|Santonian|Type Section: MacIntyre Gully; 31o19'S 115o54'E. 19m thick marine shelf deposits; highly fossiliferous.||Coolyena Group||Overlies Molecap Greensand conformably. Overlain by Poison Hill Greensand conformably.|White or grey chalk, slightly glauconitic; occasionally glauconitic marl.|
7259|Gingin Chalk|44657|14|Not recorded|p.12|||||||||
7259|Gingin Chalk|44995|14|Not recorded|p.6-198||Late Cretaceous|U.Cretaceous forams.||||||
7259|Gingin Chalk|44996|14|Not recorded|p.316||Santonian|Perth Basin.||||||
7259|Gingin Chalk|46883|6|Mentioned|p211|||||||||
7259|Gingin Chalk|48831|14|Not recorded|p.21|||||||||
7259|Gingin Chalk|48848|14|Not recorded|p.5,62,65,68,81-88|||||||||
7259|Gingin Chalk|48925|6|Mentioned|p7|||Upper Cretaceous - Santanian age. Fauna.P12 etc.||||||
7259|Gingin Chalk|48971|6|Mentioned|p51|||See also P54, P55, P56, P57, P58.||||||
7259|Gingin Chalk|60726|5|Briefly described|p5, throughout text. |Santonian|Santonian|Contains a diverse marine biota (listed) and, according to Etheridge (1913), insects: this last is doubted by the author who searched the same quarry unsuccessfully.|||||White, friable, slightly glauconitic chalk.|
7259|Gingin Chalk|61811|4|Described|p3 Fig.2, pp15-16, pp54-57, p63.|Campanian|Santonian|Northern Perth Basin. Correlated with Toolonga Calcilutite. Contains abundant foraminiferal fauna. Type section is in MacIntyre Gully, on 'Shaddow Downs' property, 2.9 km N of Gingin post office; further details in Appendix 1. Importance in defining the Santonian-Campanian boundary is discussed.||Unit in Coolyena Group.||Overlies Molecap Greensand. Locally overlies Leederville Formation. Is overlain conformably by Poison Hill Greensand.|Fossiliferous, bioturbated chalk, locally glauconitic.|
7259|Gingin Chalk|64580|6|Mentioned|map legend|||Of Coolyena Group.||||||15-DEC-08
7259|Gingin Chalk|64635|5|Briefly described|p4 Fig.3, |Campanian|Coniacian|||Unit in Coolyena Group.||||
7259|Gingin Chalk|67340|6|Mentioned|p6|Late Cretaceous|Late Cretaceous|Northern Perth Basin.||Coolyena Group.||||
7259|Gingin Chalk|68254|6|Mentioned|p1036 Fig.2, p1046 Tb.4|Cretaceous|Cretaceous|||||||
7259|Gingin Chalk|69182|6|Mentioned|Ch2 p9, Ch2 p45, Ch2 p55, Ch2 p57|Upper Cretaceous|Upper Cretaceous|Perth Basin. ||Coolyena Group||Overlies the Molecap Greensand. Overlain by the Poison Hill Greensand.||
7259|Gingin Chalk|69297|6|Mentioned|p175, p189|Campanian|Santonian|Vlaming Sub-basin, South Perth Basin. ||Coolyena Group||Overlies the Molecap Greensand. Overlain by the Poison Hill Greensand.||
7259|Gingin Chalk|70097|5|Briefly described|p20 Fig.4|Santonian|Coniacian|Northern Perth Basin. Dandaragan Trough.||Coolyena Group||Overlies Molecap Greensand. Is overlain by Poison Hill Greensand.|Chalk.|12-SEP-17
7259|Gingin Chalk|70099|5|Briefly described|Fig.4; p6|Campanian|Santonian|Southern Perth Basin. Shallow marine sediments. Equivalent in age to deep marine, carbonate-dominated sedimentation of Mentelle 9 Supersequence.||Coolyena Group.||Overlies Molecap Greensand. Is overlain by Poison Hill Greensand.||
7259|Gingin Chalk|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greensand, chalk|
7259|Gingin Chalk|71790|6|Mentioned|p102|||Palynology p. 102.||||||
7272|Giralia Calcarenite|6876|6|Mentioned|p100 Fig.5.|Paleogene|Paleogene|The lithology was left off the diagram due to space constraints.||||||
7272|Giralia Calcarenite|12729|6|Mentioned|p9 Fig.6, p17.|Oligocene|Eocene|Shallow-marine (Hocking et al., 1987).|||||Limestone.|
7272|Giralia Calcarenite|13615|6|Mentioned|p20|||Not identified in Peedmullah Shelf area.||||||07-FEB-19
7272|Giralia Calcarenite|14228|5|Briefly described|p5 fig 2, p9, p16|Eocene|Eocene|Gascoyne Platform. Mainly preserved offshore: 78 m thick.||||Overlies Cardabia Calcarenite (disconformably). Appears to grade laterally into Robe Pisolite.|Flat-lying shallow-marine carbonate strata.|
7272|Giralia Calcarenite|22814|5|Briefly described|fig2 p247|Cenozoic|Cenozoic|||||||19-NOV-08
7272|Giralia Calcarenite|23311|5|Briefly described|map legend|Eocene|Eocene|||||||
7272|Giralia Calcarenite|23379|5|Briefly described|p159,168||Tertiary|||||||
7272|Giralia Calcarenite|23403|4|Described|p9|Eocene|Eocene|||||||24-NOV-09
7272|Giralia Calcarenite|23572|5|Briefly described|p8 Fig. 6|Oligocene|Eocene|Geological Province: Carnarvon Basin||||||
7272|Giralia Calcarenite|23620|5|Briefly described|p4 Fig. 4|Paleogene|Paleogene|||||||07-NOV-08
7272|Giralia Calcarenite|23726|5|Briefly described|p95|Eocene|Eocene|Overlying unit Mandu Limestone. Underlying unit Wilcox Formation. Geological Province: Carnarvon Basin.||||||
7272|Giralia Calcarenite|23815|4|Described|p301|Late Eocene|Middle Eocene|Of the Cardabia Group. Underlying unit: Jubilee Calcarenite (disconformable). Overlying units: Lamont Sandstone and Trealla Limestone (unconformable). Max. thickness: 226 m.||||||
7272|Giralia Calcarenite|23915|5|Briefly described|p519 Fig. 2|Paleogene|Paleogene|||||||07-NOV-08
7272|Giralia Calcarenite|23935|5|Briefly described|p11 Fig.7|Oligocene|Eocene|Geological Province: Southern Carnarvon Basin.||||||27-JAN-05
7272|Giralia Calcarenite|23976|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
7272|Giralia Calcarenite|23977|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
7272|Giralia Calcarenite|23978|5|Briefly described|Map Legend|Paleogene|Paleogene|||||||07-NOV-08
7272|Giralia Calcarenite|24059|5|Briefly described|p132|Eocene|Eocene|Geological Province: Barrow Sub-basin.||||||
7272|Giralia Calcarenite|24084|5|Briefly described|p146 Fig.2|Eocene|Eocene|Geological Province: North Carnarvon Basin.||||||16-MAR-05
7272|Giralia Calcarenite|24094|5|Briefly described|p268, p276|Middle Eocene|Middle Eocene|Of the Giralia Range Sequence. Overlies disconformably the Julbilee Calcarenite. Geological Province: Carnarvon Basin||||||16-MAR-05
7272|Giralia Calcarenite|24331|5|Briefly described|p475 Fig.2|Oligocene|Eocene|Unconformably overlies Cardabia Calcarenite. Unconformably overlain by Cape Range Group. Marine. Geological Province: Barrow Sub-basin.||||||
7272|Giralia Calcarenite|24541|4|Described|p61|Late Eocene|Middle Eocene|Geological Province: Northern Carnarvon Basin. Maximum Thickness: ~60m.||||||
7272|Giralia Calcarenite|24543|5|Briefly described|Map legend|Eocene|Eocene|Coarse foraminiferal calcarenite packstone;  minor calcirudite.||||||
7272|Giralia Calcarenite|29721|6|Mentioned|Table 102|||||||||
7272|Giralia Calcarenite|30016|6|Mentioned|p92|||Tertiary.||||||
7272|Giralia Calcarenite|30122|6|Mentioned|p42|||||||||
7272|Giralia Calcarenite|30304|5|Briefly described|p53|||Tertiary age||||||
7272|Giralia Calcarenite|30504|6|Mentioned|Fig.19|||||||||
7272|Giralia Calcarenite|30875|6|Mentioned|p10|||Upper-Middle Eocene. See also P13.||||||10-APR-08
7272|Giralia Calcarenite|31051|6|Mentioned|p83|||||||||
7272|Giralia Calcarenite|31561|6|Mentioned|p34|||Eocene - Oligocene.||||||10-APR-08
7272|Giralia Calcarenite|32117|6|Mentioned|Fig.2|||||||||
7272|Giralia Calcarenite|32166|6|Mentioned|p159|||||||||
7272|Giralia Calcarenite|32648|6|Mentioned|p32|||Eocene||||||
7272|Giralia Calcarenite|32750|6|Mentioned|p301|||Tertiary. Stratigraphy||||||
7272|Giralia Calcarenite|33386|6|Mentioned|Fig.7|||||||||
7272|Giralia Calcarenite|33453|6|Mentioned|p72|||Eocene.||||||
7272|Giralia Calcarenite|33813|6|Mentioned|p7|||||||||
7272|Giralia Calcarenite|34343|6|Mentioned|p96|||Middle Eocene. See also P102.||||||
7272|Giralia Calcarenite|34363|6|Mentioned|p57|||Eocene. See also Fig.8.||||||
7272|Giralia Calcarenite|34846|6|Mentioned|Fig.3|||||||||
7272|Giralia Calcarenite|35105|6|Mentioned|Fig.5|||||||||
7272|Giralia Calcarenite|35282|6|Mentioned|Fig.2|||||||||
7272|Giralia Calcarenite|36257|6|Mentioned|Table 2.1|||||||||
7272|Giralia Calcarenite|36890|3|Fully described|p301|||||||||
7272|Giralia Calcarenite|37016|6|Mentioned|Map legend|late Eocene|late Eocene|Middle Upper Eocene.||||||
7272|Giralia Calcarenite|37320|6|Mentioned|p237|||||||||
7272|Giralia Calcarenite|38485|4|Described|p17|||||||||
7272|Giralia Calcarenite|38773|6|Mentioned|p46|||||||||
7272|Giralia Calcarenite|39167|6|Mentioned|p68|||Foraminifera.||||||10-APR-08
7272|Giralia Calcarenite|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
7272|Giralia Calcarenite|39427|4|Described|Table 1|||||||||
7272|Giralia Calcarenite|39486|6|Mentioned|Fig.2|||||||||
7272|Giralia Calcarenite|39923|6|Mentioned|p353|||||||||
7272|Giralia Calcarenite|40342|6|Mentioned|Map legend|Eocene|Eocene|||||||
7272|Giralia Calcarenite|40343|5|Briefly described|p12|||||||||
7272|Giralia Calcarenite|40366|6|Mentioned|p91|||||||||
7272|Giralia Calcarenite|40617|6|Mentioned|p16|||||||||
7272|Giralia Calcarenite|40800|6|Mentioned|p22|||||||||
7272|Giralia Calcarenite|40992|6|Mentioned|Fig.8|||||||||
7272|Giralia Calcarenite|41271|3|Fully described|p173|||||||||
7272|Giralia Calcarenite|41437|5|Briefly described|p70|||||||||
7272|Giralia Calcarenite|41438|4|Described|p111|||||||||
7272|Giralia Calcarenite|41439|5|Briefly described|p123|||||||||
7272|Giralia Calcarenite|41443|6|Mentioned|Fig.3|||||||||
7272|Giralia Calcarenite|41444|6|Mentioned|Fig.4|||||||||
7272|Giralia Calcarenite|41729|6|Mentioned|Fig.2|||||||||
7272|Giralia Calcarenite|42075|5|Briefly described|Fig.4 P245|||||||||
7272|Giralia Calcarenite|42116|5|Briefly described|Fig.1 P6|||||||||
7272|Giralia Calcarenite|42995|5|Briefly described|Fig.8|||||||||
7272|Giralia Calcarenite|43712|6|Mentioned|Fig.10,p52||Eocene|||||||
7272|Giralia Calcarenite|43724|6|Mentioned|Fig.15,p65||Eocene|||||||
7272|Giralia Calcarenite|44159|5|Briefly described|Table p37||Middle Eocene|||||||
7272|Giralia Calcarenite|44344|14|Not recorded|p.18|||Equiv. of Merlinleigh Sandstone. (G50-1).||||||
7272|Giralia Calcarenite|44491|14|Not recorded|map legend||Late Eocene|Upper Eocene.||||||
7272|Giralia Calcarenite|44492|14|Not recorded|opp.p.4, map||Late Eocene|(F50-1,2). U.Eocene. Fauna "Indicative of marine shallow-neritic to littoral facies" (p.9).||||||
7272|Giralia Calcarenite|44532|4|Described|p.9,10, map|||(G50-5).||||||
7272|Giralia Calcarenite|44533|5|Briefly described|map legend||Eocene|Eocene.||||||
7272|Giralia Calcarenite|44537|14|Not recorded|map legend||Eocene|||||||
7272|Giralia Calcarenite|44657|14|Not recorded|p.5,6,12,13,14|||||||||
7272|Giralia Calcarenite|45015|5|Briefly described|map legend|Tertiary|Tertiary|Age is Early Tertiary.||||||01-JUN-06
7272|Giralia Calcarenite|45142|6|Mentioned|Fig.4|||||||||
7272|Giralia Calcarenite|45153|6|Mentioned|App.10-151|||||||||
7272|Giralia Calcarenite|46805|6|Mentioned|p171|||||||||
7272|Giralia Calcarenite|46808|6|Mentioned|Table 2|||||||||
7272|Giralia Calcarenite|46950|6|Mentioned|Fig.15|||||||||
7272|Giralia Calcarenite|46983|6|Mentioned|Fig.2|||||||||
7272|Giralia Calcarenite|48610|14|Not recorded|p14|||Salt Marsh area.||||||
7272|Giralia Calcarenite|48831|14|Not recorded|p.80,84|||||||||
7272|Giralia Calcarenite|49942|5|Briefly described|p4 Fig.3|Oligocene|Eocene|Geological Province: Gascoyne Platform.||||||
7272|Giralia Calcarenite|50085|5|Briefly described|p23 Fig. 12|Paleogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
7272|Giralia Calcarenite|60384|6|Mentioned|p244, p243 Fig 2a|Oligocene|Eocene|Carnarvon Basin.||||||
7272|Giralia Calcarenite|61023|5|Briefly described|p27 Fig. 12|Paleogene|Paleogene|Geological Province: Northern Carnarvon Basin.||||||07-NOV-08
7272|Giralia Calcarenite|61155|5|Briefly described|p15|Late Eocene|Middle Eocene|Overlain by, and interfingered with, Merlinleigh Sandstone. Age: 47.5-38.5Ma. Max. thickness: 226m. Geological Province: Carnarvon Basin/onshore.||||||03-MAR-10
7272|Giralia Calcarenite|61958|5|Briefly described|Map sheet 1|Paleogene|Paleogene|||||||
7272|Giralia Calcarenite|62734|5|Briefly described|p1362 Fig. 2|Oligocene|Eocene|Geological Province: Barrow Sub-basin.||||||10-APR-08
7272|Giralia Calcarenite|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: 50-35Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
7272|Giralia Calcarenite|64977|6|Mentioned|p493 Fig.3.|Paleogene|Paleogene|Thevenard Island area.||||Unconformably overlies Cardabia Calcarenite. Is unconformably overlain by Cape Range Group.||
7272|Giralia Calcarenite|65891|5|Briefly described|p221 Fig.5, p224, p227. |Paleogene|Paleogene|Southern Carnarvon Basin. Marks the beginning of late Eocene carbonate accumulation after a gap and erosion in the Lutetian. Is overlain by an isolated, weathered remnant of a siliceous unit.||||||
7272|Giralia Calcarenite|66125|5|Briefly described|p132|||Giralia Anticline.|||||Mixed glauconitic/phosphatic sands interbedded with chalky skeletal packstones/wackestones in which bryozoans, echinoids and foraminifers are common.|
7272|Giralia Calcarenite|67200|5|Briefly described|p8 fig 6, p53|Eocene|Eocene|Thermal conductivity of 1.68 W/mK||||Overlain by Mandu Limestone|Crudely bedded calcarenite and limestone.|
7272|Giralia Calcarenite|69182|6|Mentioned|Ch3 p8, Ch3 p12-p13, Ch3 p23|Upper Eocene|Middle Eocene|Carnarvon Basin. Maximum thickness of 78m. See also Ch3 p35, Ch3 p37, Ch3 p53, Ch3 p65-p66, Ch3 p69, Ch3 p71, Ch3 p73.||||Disconformably overlies the Cardabia Calcarenite. Overlies the Korojon Calcarenite. Grades laterally into the Robe Pisolite. Overlain by the Mandu Calcarenite.||
7272|Giralia Calcarenite|69297|5|Briefly described|p247, p249|Cenozoic|Cenozoic|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Unconformably overlies the Miria Formation. Unconformably overlain by the Trealla Limestone.|Calcarenite.|
7272|Giralia Calcarenite|69558|5|Briefly described|p98|Eocene|Eocene |Exposed at a few localities east of Hamelin Pool. ||||Overlies the Toolonga Calcilutite.|Greenish-gray calcarenite.|
7272|Giralia Calcarenite|70066|5|Briefly described|Dampier: Fig.2. Regional: Fig.6|Priabonian|Lutetian|Northern Carnarvon Basin.||||Overlies Wilcox Formation or Cardabia Calcarenite. Is overlain by Mandu Limestone.||
7272|Giralia Calcarenite|70826|6|Mentioned|p7 tbl 4|Eocene|Eocene|Northern Carnarvon Basin.||||||
7272|Giralia Calcarenite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcarenite|
7272|Giralia Calcarenite|72034|5|Briefly described|500k_interpgeop16_lut|Eocene|Eocene|Marine, coastal, and continental deposits, Northern Carnarvon Basin.  Age from biostratigraphy.|||||Coarse-grained foraminiferal calcarenite packstone, minor calcirudite, common ferruginous grains.|
7320|Glass Spring Formation|22589|6|Mentioned|p125||Proterozoic|||||||
7320|Glass Spring Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
7320|Glass Spring Formation|22901|6|Mentioned|76 fig 2|||Geol province Officer Basin||||||
7320|Glass Spring Formation|22907|6|Mentioned|41|||||||||
7320|Glass Spring Formation|23156|4|Described|p9 & p12|Neoproterozoic|Neoproterozoic|For location of type section see p12.  Unit contains cross-bedding that indicates a strong unidirectional flow. Unit defined by Williams (1992).||||||22-FEB-17
7320|Glass Spring Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
7320|Glass Spring Formation|24018|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. Geological Province: Officer Basin.||||||
7320|Glass Spring Formation|42708|5|Briefly described|Plate 1|Proterozoic||Reserved as Glass Spring.||||||
7320|Glass Spring Formation|43209|5|Briefly described|map legend||Neoproterozoic|Of Savory Group.||||||
7320|Glass Spring Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|of Savory Group||||||
7320|Glass Spring Formation|43492|4|Described|9|||||||||
7320|Glass Spring Formation|43756|6|Mentioned|Fig.1,p535|||||||||
7320|Glass Spring Formation|44111|6|Mentioned|p.58, Fig. 2|||in Savory Basin||||||
7320|Glass Spring Formation|50195|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group (Bangemall Supergroup).  Poorly sorted, cross-bedded sandstone and pebbly conglomerate.  Geological Province: Salvation Basin.||||||
7320|Glass Spring Formation|50334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Sunbeam Group. Geological Province: Officer Basin, Centralian Superbasin.||||||
7320|Glass Spring Formation|62453|6|Mentioned|p52|||Of the Salvation Group.||||||
7320|Glass Spring Formation|64580|4|Described|map legend||Mesoproterozoic|Of Salvation Group. Sandstone; minor conglomerate and siltstone.||||||09-DEC-08
7320|Glass Spring Formation|64772|5|Briefly described|p13, p25 Fig. 12, Plate 1|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group. Sandstone; minor conglomerate and siltstone. See also p72-74 Fig.4.1.||||||25-NOV-13
7320|Glass Spring Formation|64793|6|Mentioned|p283 fig 2|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
7320|Glass Spring Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin. Arenaceous. Part of Supersequence 1.||||||
7320|Glass Spring Formation|65416|5|Briefly described|p140.|Neoproterozoic|Neoproterozoic|Savory Sub-basin. Correlated with Townsend Quartzite. Deposited by westward-directed palaeocurrents in a transgressive, shallow-water, marine shelf environment.||||Is overlain by Jilyili Formation.|Medium- to coarse-grained sandstone and siltstone, with scattered conglomerate lenses at the base.|
7320|Glass Spring Formation|69091|5|Briefly described|p202|Mesoproterozoic|Mesoproterozoic|Salvation Basin. Age: late Mesoproterozoic|||||Siliciclastic sedimentary rocks.|
7320|Glass Spring Formation|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Unit of Salvation Group.||||
7320|Glass Spring Formation|70768|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Salvation Basin.|1229-1080 Ma.|Salvation Group.||Is faulted against Calyie Formation (Collier Group).|Sandstone; minor conglomerate and siltstone.|25-NOV-16
7320|Glass Spring Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sandstone|
7320|Glass Spring Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Salvation Basin. ||Salvation Group|||Sandstone; minor conglomerate and siltstone.|
7321|Glasse Formation|22583|5|Briefly described|381|Archean|Archean|Geol province Yigarn Craton. Max thickness 1500m. Underlying unit Honman Formation||||||07-NOV-08
7321|Glasse Formation|23129|5|Briefly described|p358|||||||||
7321|Glasse Formation|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
7321|Glasse Formation|31093|2|Defined|p10|Neoarchean|Neoarchean|||||||07-NOV-08
7321|Glasse Formation|65487|5|Briefly described|p5|||Part of the Lake Johnston Greenstone Belt, locally folded into the Burmister Syncline and the Gordon Anticline. Consists of metamorphosed mafic volcanics, mafic intrusive and ultramafic rocks.||||||
7321|Glasse Formation|68520|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 3 facies variants are mapped separately.|||||Fine- to medium-grained amphibolite; amphibolite after mafic volcanic rocks; aphyric to fine-grained basalt, locally amygdaloidal, metamorphosed.|
7321|Glasse Formation|69404|5|Briefly described|p8 Fig.9|||Lake Johnston greenstone belt, Southern Cross Domain. Younger than 2873 Ma on the basis of stratigraphic relationship with the Honman Formation. Approximately 2km thick.||||Overlies the Honman Formation|Pillowed and massive basalts with minor ultramafic intrusions.|
7321|Glasse Formation|69559|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. See also geologyp_lut.csv, geologyp_lut.csv, 500k_interpgeop_lut.csv.|2873-2720 Ma||||Fine to medium grained amphibolite after mafic volcanic rock. Aphyric to fine grained basalt, locally amygdaloidal; metamorphosed.|
7321|Glasse Formation|69617|5|Briefly described|p145-148, p154-155|||Lake Johnston greenstone belt, Youanmi Terrane, Yilgarn Craton. Up to 1200m thick. Deposited above the Roundtop Komatiite: possible age discussed.|||||Deformed and massive, fine-grained green-grey metabasalt. Contains rare horizons with amygdales to 5mm and relict feldspar phenocrysts; cut by deformed quartz veins.|
7321|Glasse Formation|70144|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton.|||||Aphyric to fine-grained basalt, locally amygdaloidal; metamorphosed.|
7321|Glasse Formation|70153|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean||2873 - 2720 Ma (inferred).||||Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed.|
7321|Glasse Formation|70156|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3200-2600 Ma). See 500k_interpgeop14_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|2873-2720 Ma (inferred)||||Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed|
7321|Glasse Formation|70205|5|Briefly described|Map legend.|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton.|||||Fine- to medium-grained amphibolite.|
7321|Glasse Formation|70277|6|Mentioned|p799-800|Archean|Archean|Geological province: Yilgarn Craton. Part of the ~2.9 Ga Lake Johnston greenstone belt.|||||Pillowed basalt with minor ultramafic intrusions.|
7321|Glasse Formation|70794|5|Briefly described|100k_geologyp_lut.csv|Neoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Age range 2873-2720 Ma shown in 500k_interpgeop14_lut.csv. See also  500k_interpgeop_lut.csv.|2920-2718 Ma inferred||||Amphibolite after mafic volcanic rock. Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed.Fine to medium grained amphibolite.|
7321|Glasse Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|2873-2720 Ma (inferred)||||Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed|
7321|Glasse Formation|71270|4|Described|500k_interpgeop16_lut.csv|Mesoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Youanmi Terrane events (3131 - 2600 Ma).|2920-2718 Ma (inferred)||||Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed|
7321|Glasse Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|||||Aphyric to fine-grained basalt; locally amygdaloidal; metamorphosed.|
7349|Glen Ross Shale Member|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. Overlying unit Kiangi Creek Formation. U'lying unit Irregully Formation. Geological Province: Bangemall Basin. Max. thickness: >525 m.||||||
7349|Glen Ross Shale Member|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7349|Glen Ross Shale Member|35982|6|Mentioned|p136|||||||||
7349|Glen Ross Shale Member|36551|6|Mentioned|p101|||See also P22.||||||
7349|Glen Ross Shale Member|37328|6|Mentioned|p4|||||||||
7349|Glen Ross Shale Member|39171|6|Mentioned|p80|||See Fig. 50||||||
7349|Glen Ross Shale Member|40089|4|Described|p26|||Of Kiangi Creek Formation.||||||03-FEB-12
7349|Glen Ross Shale Member|44142|6|Mentioned|p313 Tb.4-4|||Occurs in Mount Vernon Syncline.||Kiangi Creek Formation.||||
7417|Glenhill Formation|22547|4|Described|p26|Tonian|Stenian|Of the Carr Boyd Group;  Carr Boyd Basin. Age: 1057 +/- 80 Ma. Thickness: 300 m. Overlies Lissadell Formation, overlain by Antrim Plateau Volcanics||||||19-SEP-06
7417|Glenhill Formation|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group.||||||
7417|Glenhill Formation|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
7417|Glenhill Formation|32660|5|Briefly described|Table 6|||||||||
7417|Glenhill Formation|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
7417|Glenhill Formation|32728|5|Briefly described|Table 6|||See also p47.||||||19-SEP-06
7417|Glenhill Formation|36551|6|Mentioned|Table 12|||||||||
7417|Glenhill Formation|36885|4|Described|p179|||||||||
7417|Glenhill Formation|37462|6|Mentioned|Fig.4.13|||||||||
7417|Glenhill Formation|40813|6|Mentioned|p335|||||||||
7417|Glenhill Formation|41158|6|Mentioned|p37|||||||||
7417|Glenhill Formation|43853|5|Briefly described|Map Legend||Proterozoic|||||||
7417|Glenhill Formation|44155|5|Briefly described|p250 Tb.3-10|||600-1500m thick.||Carr Boyd Group||Unconformably overlies Lissadell Formation. Correlated with Glidden Group.|Red, green and black, commonly laminated siltstone, shale and fine sandstone (locally glauconitic); blocky quartz sandstone.|
7417|Glenhill Formation|44230|5|Briefly described|Map Legend||Proterozoic|||||||
7417|Glenhill Formation|44363|4|Described|p.6,14,17|||(Adelaidean). Of the Carr Boyd Group.||||||19-SEP-06
7417|Glenhill Formation|44364|14|Not recorded|map legend||Proterozoic|||||||
7417|Glenhill Formation|45047|4|Described|p35|||||||||
7417|Glenhill Formation|45112|6|Mentioned|Table 16|||||||||
7417|Glenhill Formation|65417|5|Briefly described|pp156-159.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Age from Bofinger (1967) recalculated by Plumb et al. (1981). Braided-delta progradation and retreat.|1057 +/- 80 Ma (Rb-Sr whole rock).|Unit in Carr Boyd Group.||Conformably overlies Lissadell Formation. Is overlain conformably by Stonewall Sandstone.||
7417|Glenhill Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin||Carr Boyd Group|Includes unnamed sandstone member||Micaceous siltstone, fine- to coarse-grained quartz sandstone, and mudstone.|31-JUL-15
7417|Glenhill Formation|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Micaceous siltstone, fine to coarse grained quartz sandstone and mudstone.|
7417|Glenhill Formation|69435|5|Briefly described|p20:3|||Carr Boyd Basin.||Carr Boyd Group.||Overlies Lissadell Formation. Is overlain by Stonewall Sandstone.||12-JUL-16
7417|Glenhill Formation|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1200-1177 Ma (Inferred)|Unit of Carr Boyd Group.|||Micaceous siltstone, fine- to coarse-grained quartz sandstone, and mudstone|
7417|Glenhill Formation|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Stonewall Sandstone, overlies Lissadell Formation||
7417|Glenhill Formation|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1177-1200 Ma|Carr Boyd Group|||Micaceous siltstone, fine to coarse grained quartz sandstone and mudstone.|
7417|Glenhill Formation|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1200-1177 Ma (inferred)|Unit of Carr Boyd Group.|||Micaceous siltstone, fine- to coarse-grained quartz sandstone, and mudstone|
7456|Glyde Formation|30385|4|Described|p8|||||||||
7456|Glyde Formation|30388|4|Described|Table 1|||Middle Proterozoic. Table 1 on P8. Pussy Cat Group.||||||
7456|Glyde Formation|30390|4|Described|p50|||||||||
7456|Glyde Formation|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7456|Glyde Formation|30946|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Of Pussy Cat Group.||||||
7456|Glyde Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7456|Glyde Formation|36551|6|Mentioned|Table 31|||||||||
7456|Glyde Formation|36886|4|Described|p199|||||||||
7456|Glyde Formation|65256|6|Mentioned|p14, p32|||Of the Pussy Cat Group. A succession of interlayered siltstone, shale, dolomite and epidotised amygdaloidal basalt. May be equivalent to Tjuninanta Formation of Tjauwata Group.||||||
7456|Glyde Formation|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.||Unit in Pussy Cat Group.|||Mafic volcanic, volcaniclastic and clastic rocks.|11-APR-12
7456|Glyde Formation|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Mapped as three separate but un-named units.|1072 - 1065 Ma.|Unit in Pussy Cat Group.|||Vesicular and amygdaloidal basalt, basaltic andesite, and andesite; ahpyric rhyolitic and trachydacitic volcanic siltstone and mudstone; interlayered sandstone, well- to very poorly-sorted conglomerate, and basalt.|
7456|Glyde Formation|67375|4|Described|p19 Fig.11, p38 Table 1, p47. |Mesoproterozoic|Mesoproterozoic|The volcaniclastic metasedimentary rocks of the lower part of this unit were deposited in a volcanically active alluvial to fluviolacustrine environment.|1071-1065 Ma.|Unit in Pussy Cat Group.||Intercalated with and overlies Kathleen Ignimbrite. Is overlain by Wururu Rhyolite or Gurgadi Basalt.|Low-grade metamorphic, volcaniclastic sedimentary rocks: mudstones, siltstones and shales; arkosic or calcareous sandstones, and diamictites; overlain by amygdaloidal metabasaltic lavas.|
7456|Glyde Formation|67553|4|Described|p20-21,40,44,48-51,94,97-100,104-106|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Depositional age at 1070+\-5 Ma (GSWA 195723) coeval with eruption of Kathleen Ignimbrite. Juxtaposed against diamictite in the upper Mount Palgrave Group as a result of NW-trending faulting and reactivation of earliers sub-volcanic block faults at <1055+\-10 Ma. Outcrop as a conspicuous, recessive, NNE-trending band along the northern side of the Mount Glyde Ranges. Lower siliciclastic section deposited in a volcanically active alluvial to fluviolacustrine environment. Upper section was erupted and deposited subaerially, and entered bodies of water forming local occurrences of pepperites and hyaloclastics. Underwent moderate temperature, LP metamorphism.|1070+\-5 Ma|Unit of Pussy Cat Group.||Uppermost unit of Pussy Cat Group. Overlain by Wururu Rhyolite or Gurgadi Basalt/Cassidy Group. Intruded by the Kathleen Ignimbrite.|Massive to laminated mudstones, siltstones, and shales; well to poorly sorted, partly arkosic or calcareous sandstones; conglomerates; and very poorly sorted, matrix-supported diamictites. Extrusive amygdaloidal to massive metabasaltic lava.|06-AUG-19
7456|Glyde Formation|68995|5|Briefly described|p15, p49 Fig.25|||Primarily erupted in a sub-aerial environment, but locally some lavas entered small water bodies where they formed peperites and hyaloclastites.||Pussy Cat Group||Overlies the Kathleen Ignimbrite.|Massive and amygdaloidal, mostly aphyric, basaltic lavas intercalated with minor amounts of metasedimentary rocks, including siltstone, quartzite and siliceous microbialites.|
7456|Glyde Formation|68996|5|Briefly described|p7|Mesoproterozoic|Mesoproterozoic|||Pussy Cat Group|||Mafic volcanic and volcaniclastic sedimentary rocks.|
7456|Glyde Formation|69003|5|Briefly described|p51|Mesoproterozoic|Mesoproterozoic|Southern Talbot Sub-basin.||Pussy Cat Group.||Intercalated with Glyde Formation.|Volcaniclastic rocks and minor amygdaloidal basalt; intercalated with flow-banded ignimbrites of the Kathleen Ignimbrite.|
7456|Glyde Formation|69091|5|Briefly described|p71 Fig.4.14, p76|||Talbot Sub-basin||Pussy Cat Group|||Basalt dominated sequence and volcaniclastic dominated sequence.|
7456|Glyde Formation|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample description includes: metamafic volcanic rock; dark-coloured; fine-grained volcaniclastics (mudflow and floodplain deposits) with a dominantly mafic volcanic source; altered by contact metamorphism to biotite-rich microgranofelses; meta-igneous mafic volcanic; meta-sedimentary.||Pussy Cat Group|||Vesicular and amygdaloidal basalt, andesite, and basaltic andesite; interbedded with siliciclastic rocks; epidotized|
7456|Glyde Formation|69655|6|Mentioned|p57|||||Bentley Supergroup||||
7456|Glyde Formation|69729|5|Briefly described|p82|||Bedrock of Talbot Sub-basin.||Pussy Cat Group.|||Volcaniclastics- and basalt-dominated sequences.|
7456|Glyde Formation|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The two facies are mapped separately.|c.1065 Ma.|Pussy Cat Group.|||Vesicular and amygdaloidal basalt, and minor basaltic andesite, interbedded with fine- to coarse-grained siliciclastic rocks, epidotised; vesicular and amygdaloidal basalt, basaltic andesite and andesite, locally plagioclase-phyric (section only).|
7456|Glyde Formation|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Three facies associations are mapped separately.|1071-1047 Ma.|Pussy Cat Group.||Overlies Mount Waugh Formation. Is overlain by Wururu Rhyolite. Is intruded by Warakurna Supersuite.|Typically vesicular and amygdaloidal basalt, and minor basaltic andesite; interbedded with fine- to coarse-grained siliciclastic rocks; epidotised.|
7456|Glyde Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Bentley Supergroup|||Vesicular and amygdaloidal basalt plagioclase porphyritic basalt, basalt, basaltic andesite and andesite. Diamictite with sub-rounded to angular, mafic-felsic volcanic clasts. Medium-fine grained siliclastic rocks; rare calc-silicate rocks.|
7456|Glyde Formation|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Basalt, and minor basaltic andesite, plagioclase porphyritic basalt, vesicular and magdaloidal basalt, andesite, medium- to fine-grained siliciclastic rocks; rare calc-silicate rocks, diamictite, evaporite horizons and microbialites.|
7456|Glyde Formation|71211|5|Briefly described|p26-p28, p30, p86|||See also p87 fig 3.2, p135, p137 fig 4.2, p138, p216. ||||Overlies the Cleghorne Formation. Intruded by the Rowland Suite.|Massive basalt and interbedded volcaniclastic rocks.|
7456|Glyde Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||ash tuff, shale, siltstone, basalt|
7456|Glyde Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Basalt; vesicular, amyddaloidal, palgioclase porphyritic, and minor basaltic andesite; diamictite, medium- to fine-grained siliciclastics, evaporites and microbialites.|
7456|Glyde Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Pussy Cat Group|||Typically vesicular and amygdaloidal basalt, and minor basaltic andesite; interbedded with fine- to coarse-grained siliciclastic rocks; epidotized.|
7456|Glyde Formation|72443|6|Mentioned|p738|||||Pussy Cat Group||||
7463|Gneudna Formation|1943|5|Briefly described|p388-389, p376, p377 Fig. 5|||||||Correlation with Sweeney Mia Formation preferred. Overlies Nannyarra Formation in Pendock-1A.||
7463|Gneudna Formation|6943|6|Mentioned|p602.|||Carnarvon Basin.||||Overlies Nannyarra Formation.||
7463|Gneudna Formation|6944|5|Briefly described|p571, p583, p585 Table 1.|Late Devonian|Middle Devonian|Late Givetian to Early Frasnian. Grades up from underlying Nannyarra Formation; its base is the first limestone bed. Underlies Munabia Formation. Includes Point Maud Member. Shale and wackestone, bioturbated packstone and coarse grainstone.||||||23-SEP-15
7463|Gneudna Formation|12471|5|Briefly described|p475 Fig.2. |Late Devonian|Middle Devonian|Oil extracts were considered to be mature migrated crudes, sourced from algal/carbonate-rich rocks of Devonian to Siluro-Ordovician age.||||Overlies Nannyarra Sandstone.||
7463|Gneudna Formation|12729|4|Described|Throughout|Famennian|Givetian|Deposited in a nearshore to restricted shallow-marine environment. 358 m thick in Gneudna 1, near Williambury Station type section. 1092 m thick (max). Optivus-triangulatus Zone palynomorphs(late Givetian - early Frasnian). Abundant skeletal debris. Unit sequence stratigraphy see Gorter et al. (1998).|||Point Maud Member|Conformably underlies the Munabia Sandstone, conformably overlies the Nannyarra Sandstone.|Interbedded carbonate and siltstone with minor evaporite.|
7463|Gneudna Formation|12731|5|Briefly described|p590 Fig.2.|Late Devonian|Middle Devonian|Organic-rich beds are more mature in northern part of Gascoyne Platform. Dolomite might be a potential hydrocarbon reservoir.||||Overlies Nannyarra Sandstone. Is overlain by Munabia Sandstone.|Shelf carbonates, thin organic-rich shale beds.|
7463|Gneudna Formation|12733|5|Briefly described|p554 Fig.2, pp556-565.|Late Devonian|Middle Devonian|Givetian-Frasnian. Oil and gas source in Gascoyne Platform, Merlinleigh Sub-basin and Peedamullah Shelf. Expected to act as source and seal for Nannyarra Sandstone. Petroleum generating potential is fair to excellent.||||Overlies Nannyarra Sandstone. Is overlain by Munabia Sandstone.|Shallow-marine to intertidal carbonates and fine-grained siliciclastics.|
7463|Gneudna Formation|13615|3|Fully described|p4, p6-8, p16, p73-75|Famennian|Frasnian|Peedamullah Shelf. Up to 794m thick. Spores and Pollen zone provided. Type section occurs Southeast of Williambury Homestead at 23deg58'10"S 115deg12'30"E. Contains rich and diverse fauna. Deposited in a marine shelf to intertidal environment. See also p78, p80, p83, p87, p103, 104 App. 3, p118, Plates 2, 3. Misspelt Gueudna Formation p34.|c. 375 Ma|||Conformably overlies the Nannyarra Sandstone. Disconformably overlain by the Moogooree Limestone.|Limestone, mostly packstone and locally dolomitized, lesser sandstone and siltstone.|07-FEB-19
7463|Gneudna Formation|14228|5|Briefly described|p1, p3, p5 fig2, p6 fig3, p16-21|Frasnian|Givetian|Gascoyne Platform and Merlinleigh Sub-basin. Petroleum source beds. Nearshore marine environment. Max thickness 1092m. Maturity increases to north. Intraformational shales could be a seal for this unit and the underlying Nannyarra Sandstone.|||Point Maud Member|Overlies/ grades into Nannyarra Sandstone conformably. Conformably overlain by or interfingers with Munabia Formation.|Interbedded carbonate and siltstone.|
7463|Gneudna Formation|22814|5|Briefly described|p250, fig2|Devonian|Devonian|||||||
7463|Gneudna Formation|22817|6|Mentioned|p2|Devonian|Devonian|||||||
7463|Gneudna Formation|23311|5|Briefly described|map legend|Frasnian|Early Devonian|||||||
7463|Gneudna Formation|23312|5|Briefly described|map legend|Frasnian|Early Devonian|||||||
7463|Gneudna Formation|23572|4|Described|p8 Fig. 6, p11|Frasnian|Givetian|Geological Province: Carnarvon Basin. Underlying Unit: Nannyarra Sandstone (conformable). Overlying Unit: Munabia Sandstone (conformable).||||||
7463|Gneudna Formation|23726|5|Briefly described|p32|Devonian|Devonian|Overlying unit Munabia Sandstone. Underlying unit Nannyarra Sandstone. Geological Province: Carnarvon Basin.||||||
7463|Gneudna Formation|23815|4|Described|p273|Frasnian|Givetian|Geological Province: Carnarvon Basin. Underlying unit: Nannyarra Greywacke (conformable). Overlying unit: Munabia Sandstone (confromable). Max. thickness: 820 m. Richly fossiliferous.||||||
7463|Gneudna Formation|23935|4|Described|p11 Fig.7|Famennian|Givetian|Conformably overlies Nannyarra Sandstone. Conformably overlain by Munabia Sandstone. Geological Province: Southern Carnarvon Basin.||||||
7463|Gneudna Formation|24390|5|Briefly described|p19 Fig. 10|Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
7463|Gneudna Formation|30875|6|Mentioned|p10|||Middle to Upper Devonian. See also P14||||||
7463|Gneudna Formation|31055|6|Mentioned|p588|||Middle Devonian||||||
7463|Gneudna Formation|31150|6|Mentioned|p98|||Refers Balme (1960)||||||
7463|Gneudna Formation|31152|6|Mentioned|p6|||||||||
7463|Gneudna Formation|31250|6|Mentioned|p10|||||||||
7463|Gneudna Formation|31561|5|Briefly described|p33|||Late Devonian. See also P34||||||
7463|Gneudna Formation|32619|6|Mentioned|p463|||Givetian-Frasnian. Fauna. See also P464.||||||
7463|Gneudna Formation|32640|6|Mentioned|p236|||||||||
7463|Gneudna Formation|32648|6|Mentioned|p32|||Dev.||||||
7463|Gneudna Formation|32865|4|Described|p477|||Early Frasnian||||||
7463|Gneudna Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
7463|Gneudna Formation|33042|6|Mentioned|p732|||See also P733,740,753, & Pl.16.||||||
7463|Gneudna Formation|33386|6|Mentioned|Fig.7|||||||||
7463|Gneudna Formation|33435|6|Mentioned|p130|||Devonian.||||||
7463|Gneudna Formation|33453|5|Briefly described|p69|||Devonian.||||||
7463|Gneudna Formation|33625|6|Mentioned|Fig.8|||||||||
7463|Gneudna Formation|34287|6|Mentioned|p93|||||||||
7463|Gneudna Formation|34484|6|Mentioned|p21|||Latest Givetian &/or earliest Frasnian||||||
7463|Gneudna Formation|34999|6|Mentioned|p124|||||||||
7463|Gneudna Formation|35282|6|Mentioned|p1|||||||||
7463|Gneudna Formation|35981|6|Mentioned|p135|||||||||
7463|Gneudna Formation|36257|6|Mentioned|Table 2.1|||||||||
7463|Gneudna Formation|36293|6|Mentioned|p81|||||||||
7463|Gneudna Formation|36743|4|Described|p41|||||||||
7463|Gneudna Formation|36890|3|Fully described|p275|||See also P230.||||||
7463|Gneudna Formation|36902|6|Mentioned|p22|||||||||
7463|Gneudna Formation|38482|6|Mentioned|p22|||See Table 10||||||
7463|Gneudna Formation|38593|6|Mentioned|p87|||Carnarvon Basin||||||
7463|Gneudna Formation|38770|5|Briefly described|Fig.1|||||||||
7463|Gneudna Formation|39427|4|Described|Table 1|||||||||
7463|Gneudna Formation|40617|6|Mentioned|p15|||Mention Fig.1||||||
7463|Gneudna Formation|40992|6|Mentioned|Fig.8|||||||||
7463|Gneudna Formation|41271|3|Fully described|p45|||Formerly Gneudna Limestone.||||||15-DEC-08
7463|Gneudna Formation|41438|6|Mentioned|p102|||||||||
7463|Gneudna Formation|41441|5|Briefly described|p151|||||||||
7463|Gneudna Formation|41443|5|Briefly described|p159|||||||||
7463|Gneudna Formation|41492|4|Described|p110|||||||||
7463|Gneudna Formation|41512|4|Described|p29|||||||||
7463|Gneudna Formation|41672|5|Briefly described|p160|||||||||
7463|Gneudna Formation|42030|3|Fully described|p744|||||||||
7463|Gneudna Formation|42111|6|Mentioned|p104|||||||||
7463|Gneudna Formation|42116|4|Described|p24|||See also Fig.9||||||
7463|Gneudna Formation|42194|6|Mentioned|p31|||||||||
7463|Gneudna Formation|42230|4|Described|p127|||||||||
7463|Gneudna Formation|42351|5|Briefly described|p46|||Carnarvon Basin||||||
7463|Gneudna Formation|42482|6|Mentioned|p103|||||||||
7463|Gneudna Formation|42564|6|Mentioned|p11|||Carnarvon Basin.||||||
7463|Gneudna Formation|42994|5|Briefly described|p86|||||||||
7463|Gneudna Formation|43566|6|Mentioned|p413|||||||||
7463|Gneudna Formation|43825|6|Mentioned|p144||Devonian|||||||
7463|Gneudna Formation|43914|14|Not recorded|p7,17,25,26|||||||||
7463|Gneudna Formation|44220|14|Not recorded|p.69,70,78||Frasnian|||||||
7463|Gneudna Formation|44344|14|Not recorded|p.5,20,24,opp.4,map||Frasnian|(Frasnian). (G50-1).||||||
7463|Gneudna Formation|44345|14|Not recorded|map legend||Late Devonian|Upper Devonian.||||||
7463|Gneudna Formation|44537|14|Not recorded|map legend||Middle Devonian|Middle Devonian.||||||
7463|Gneudna Formation|44657|14|Not recorded|p.5,7,8,15|||||||||
7463|Gneudna Formation|44993|14|Not recorded|p.7,18-23,26,30-1,36|||On many pages.||||||
7463|Gneudna Formation|44994|5|Briefly described|p9|||Devonian.||||||
7463|Gneudna Formation|45015|2|Defined|p39-48, map legend|Devonian|Devonian|Calcarenite, quartzwacke. calcilutite and calcareous siltstone, generally very fossiliferous. Overlies conformably, Nannyarra Greywacke; conformably underlies Munabia Sandstone. Max. thickness: 2700ft. Geol.Prov: Carnarvon Basin. See also p53 Fig. 21.||||||29-JAN-08
7463|Gneudna Formation|45016|14|Not recorded|p9,21,24,25,34||Devonian|||||||
7463|Gneudna Formation|45040|14|Not recorded|p68||Devonian|||||||
7463|Gneudna Formation|45041|6|Mentioned|Fig.45|||Frasnian||||||
7463|Gneudna Formation|45063|6|Mentioned|p30|||See also Fig. 9. Devonian||||||
7463|Gneudna Formation|45101|6|Mentioned|p46|||||||||
7463|Gneudna Formation|46973|6|Mentioned|p51|||||||||
7463|Gneudna Formation|48610|14|Not recorded|p14|||Salt Marsh area.||||||
7463|Gneudna Formation|48628|14|Not recorded|p.1,4,5|||||||||
7463|Gneudna Formation|48831|14|Not recorded|p.50|||On many pages. p.44,46-48,50,59-61,64,67,71.||||||
7463|Gneudna Formation|48848|14|Not recorded|p.14-16,19,20,59|||||||||
7463|Gneudna Formation|48971|6|Mentioned|p10|||See also P27.||||||
7463|Gneudna Formation|49942|4|Described|p4 Fig.3, p9|Late Devonian|Late Devonian|Conformably overlies Nannyarra Sandstone. Conformably overlain by Munabia Formation, locally interfingering. Max. thickness: 1092 m. Interbedded carbonate rocks and siltstone with minor evaporites.  Geological Province: Gascoyne Platform.||||||
7463|Gneudna Formation|50085|5|Briefly described|p19 Fig. 10, p20 Tb. 5|Late Devonian|Devonian|Geological Province: Southern Carnarvon Basin.||||||
7463|Gneudna Formation|60384|5|Briefly described|p244, p243 Fig 2a, p250, 251, p260|Late Devonian|Late Devonian|Southern Carnarvon Basin. Minor oil show at top|||||Interbedded carbonates and siltstone with minor evaporites|
7463|Gneudna Formation|60725|5|Briefly described|p29-31; p33-37; p39.|Frasnian|Givetian|Merlinleigh Sub-basin. Source beds are within the oil-generation window or overmature. Has source, reservoir and seal rocks.|||||Shallow-marine to intertidal carbonates and fine-grained siliciclastics.|10-MAY-17
7463|Gneudna Formation|61958|5|Briefly described|Map sheet 1|Devonian|Devonian|||||||21-MAR-06
7463|Gneudna Formation|64580|6|Mentioned|map legend|||Devonian succession, Southern Carnarvon Basin.||||||15-DEC-08
7463|Gneudna Formation|64783|6|Mentioned|p101|Frasnian|Givetian|Carnarvon Basin.||||||15-NOV-17
7463|Gneudna Formation|64972|6|Mentioned|p614, p617 Fig. 5, p620|Late Devonian|Middle Devonian|||||||
7463|Gneudna Formation|66127|5|Briefly described|p441.|Frasnian|Givetian|Carnarvon Basin. Palynoflora corrrelate this unit with the reef complexes in the Canning Basin, and with the Etonvale Formation of the Adavale Basin, Queensland.||||||
7463|Gneudna Formation|66498|6|Mentioned|p45|Frasnian|Frasnian|Contains species-rich microvertebrate assemblages.||||||
7463|Gneudna Formation|66499|6|Mentioned|p56 Fig.1|||Carnarvon Basin||||||
7463|Gneudna Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||Includes Point Maud Member.||Light grey fine-grained sandstone with rare siltstone flasers, some slumping in adjacent core; grey calcareous? sandstone, highly fossiliferous; blue/grey limestone with common stylolites; green/grey sitlstone/claystone, some highly fossiliferous.|
7463|Gneudna Formation|67200|5|Briefly described|p7 fig 5, p48, p51, p55, app 2 p6|Devonian|Devonian|Thermal conductivity of 1.91 W/mK|||Includes Point Maud Member|Overlies Nannyarra Sandstone, overlain by Munabia Sandstone|Crudely bedded limestone with common stylolites and silststone. Fine grained sandstone with rare siltstone flasers, claystone and siltstone that is highly fossiliferous.|
7463|Gneudna Formation|68297|5|Briefly described|p183, p193|Frasnian|Givetian|Carnarvon Basin, WA. Includes youngest known thelodonts in Australia and possibly the world. ||||Conformably overlain by Munabia Sandstone||
7463|Gneudna Formation|68298|5|Briefly described|p233, p234, p250 App. 1|Frasnian|Frasnian|Diverse macrovertebrate fauna contains Groenlandaspis sp., eubrachythoracid anthrodires, Chirodipterus australia and other chirodipterids (Long, 1987c) and osteolepid jaws. Marine unit.||||Is overlain by Munabia Sandstone.||
7463|Gneudna Formation|69011|5|Briefly described|Map Legend|Devonian|Devonian|Southern Carnarvon Basin.||||Overlain by the Munabia Sandstone. Underlain by the Nannyarra Sandstone.|Comprises calcareous siltstone, limestone (mostly packstone, commonly silty); siltstone, fine- to medium-grained sandstone.|24-APR-14
7463|Gneudna Formation|69029|6|Mentioned|p323,326,328|Frasnian|Givetian|Of onshore Carnarvon Basin. Contains source rock intervals of excellent to fair quality.||||Overlain by Munabia Sandstone. Underlain by Nannyarra Sandstone.||
7463|Gneudna Formation|69182|6|Mentioned|Ch3 p8, Ch3 p10-p11|Late Devonian|Late Devonian|Carnarvon Basin. Deposited in a near-shore to restricted shallow-marine environment. See also Ch3 p23, Ch3 p35, Ch3 p37, Ch3 p55, Ch3 p67-p68, Ch3 p73.  ||||Conformably overlies the Nannyarra Sandstone. Conformably overlain by (or interfingers with) the Munabia Sandstone.|Inter-bedded carbonate and siltstone.|
7463|Gneudna Formation|69297|4|Described|p246, p249-p251|Middle Devonian|Middle Devonian|Gascoyne Sub-basin of the Carnarvon Basin. Deposited in a shallow marine to coastal environment. Oil stains have been detected in this unit. This unit is a potential petroleum source rock and a good reservoir rock.  ||||Overlies the Nannyarra Sandstone. Overlain by the Gneudna Formation.|Limestones.|
7463|Gneudna Formation|69583|5|Briefly described|p133, p143|Late Devonian|Late Devonian|Gascoyne Platform, Southern Carnarvon Basin. Contains excellent to fair, but thin, source rock intervals. TOC content up to c.13%.||||||
7463|Gneudna Formation|70127|5|Briefly described|Map legend|Devonian|Devonian|Southern Carnarvon Basin.|||||Calcareous siltstone, limestone (mostly packstone, commonly silty), siltstone, fine- to medium-grained sandstone.|
7463|Gneudna Formation|70138|5|Briefly described|Map legend.|Devonian|Devonian|Southern Carnarvon Basin.||||Overlies Nannyarra Sandstone. Is overlain by Munabia Sandstone.|Calcareous siltstone, limestone (mostly packstone, commonly silty); siltstone, fine- to medium-grained sandstone.|
7463|Gneudna Formation|70795|4|Described|100k_geologyp_lut.csv|Frasnian|Frasnian|Also 100k_interpgeop_lut.csv|383-372 Ma||||Calcareous siltstone, limestone (mostly packstone, commonly silty); siltstone, fine- to medium-grained sandstone.|
7463|Gneudna Formation|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Southern Carnarvon Basin.||||||
7463|Gneudna Formation|71146|5|Briefly described|p6, p14 fig 9, p27,  p43 fig 33|Frasnian|Eifelian|Southern Carnarvon Basin. Hosts some sub-economic lead zinc deposits. Deposited in a shallow marine environment. ||||Overlies the Nanyarra Sandstone. Overlain by the Munabia Sandstone.|Carbonate and mudstone.|
7463|Gneudna Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, siltstone, limestone|
7474|Godfrey beds|7433|5|Briefly described|p25 Fig.2, p38. |Permian|Permian|See also Godfrey Beds (p32 Fig.8). Gregory Sub-basin, Canning Basin. Sandy, lagoonal? clastics. Contains intraformational mud clasts and bi-directional current ripples.||||Intercalated with/grades into Hardman Formation.|Thin-bedded quartzose sandstone sequence; abundant Rhizocorallium burrows and rare plant debris.|
7474|Godfrey beds|38878|6|Mentioned|Map legend|Tatarian|Kazanian|Kazanian - Tatarian||||||
7474|Godfrey beds|43173|6|Mentioned|54|Late Permian||||||||
7474|Godfrey beds|45153|2|Defined|App.4-81|Late Permian|Late Permian|See also App.4-74||||||
7474|Godfrey beds|45158|3|Fully described|p18|||See also p36.||||||05-NOV-15
7474|Godfrey beds|66949|4|Described|p26, p76 Appx.5, p59 Appx.3|Early Triassic|Late Permian|See also  p46 Appx.2, p60 Appx.4. McWhae et al. (1958); Casey and Wells (1964).  Appears as Godfrey Beds on p59 and just Godfrey p46, 60. Type section detailed. Up to 90m in outcrop. Stratigraphic position poorly known. Trace fossils. Available core detailed.||||Overlies Condren Sandstone. Is overlain by Millyit Sandstone. Lateral equivalent of Hardman Formation.|Sandstone, minor mudstone, and conglomerate. Includes rhizocorallid burrows and shell fragments.|05-NOV-15
7474|Godfrey beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, sandstone|
7476|Gogo Formation|6944|6|Mentioned|p582.|Late Devonian|Late Devonian|Canning Basin. Shale. Correlates with Nannyarra and Gneudna Formations of Carnarvon Basin. Best hydrocarbon source facies from Late Devonian in Canning Basin.||||||27-OCT-14
7476|Gogo Formation|12733|6|Mentioned|p565.|||Canning Basin. Contains oil-prone basal marine shales.||||||
7476|Gogo Formation|22550|6|Mentioned|Fig 3|||Informally divided into members, Fig 5||||||
7476|Gogo Formation|22741|5|Briefly described|P21, P23, Table3 P17|Givetian|Frasnian|Equivalent to Sadler Limestone.||||||10-NOV-08
7476|Gogo Formation|22767|6|Mentioned|P11|||||||||
7476|Gogo Formation|23338|5|Briefly described|915 Fig.3|Frasnian|Frasnian|||||||
7476|Gogo Formation|23356|5|Briefly described|26 Tab.2|Late Devonian|Middle Devonian|||||||
7476|Gogo Formation|23903|5|Briefly described|p1595, p1597 Fig.2|Frasnian|Givetian|Geological Province: Canning Basin||||||
7476|Gogo Formation|23979|5|Briefly described|p210|Frasnian|Givetian|Geological Province: Canning Basin.||||||19-MAY-04
7476|Gogo Formation|24000|5|Briefly described|p348 Fig. 2|Frasnian|Frasnian|Geological Province: Canning Basin.||||||
7476|Gogo Formation|24052|5|Briefly described|p167|Late Devonian|Late Devonian|Geological Province: Canning Basin. Contains lungfishes Griphognathus whitei (here described) and Chirodipterus australis.||||||08-FEB-10
7476|Gogo Formation|24061|5|Briefly described|p180|Middle Devonian|Middle Devonian|Of "Lennard River Group"?  Geological Province:  Canning Basin.||||||
7476|Gogo Formation|24224|5|Briefly described|p263|Late Devonian|Late Devonian|||||||
7476|Gogo Formation|24246|5|Briefly described|p9, 10, 11|Frasnian|Frasnian|Geological Province: Canning Basin.||||||
7476|Gogo Formation|24390|5|Briefly described|p6 Fig. 4|Devonian|Devonian|Geological Province: Canning Basin.||||||
7476|Gogo Formation|24551|6|Mentioned|p191|||||||||
7476|Gogo Formation|30181|6|Mentioned|Fig.75|||||||||
7476|Gogo Formation|30187|6|Mentioned|p179|||||||||
7476|Gogo Formation|31150|5|Briefly described|p96|||Palynology. Givetian or Frasnian age.||||||
7476|Gogo Formation|31152|6|Mentioned|p2|||||||||
7476|Gogo Formation|31332|6|Mentioned|Fig. 3|||||||||
7476|Gogo Formation|32603|6|Mentioned|p99|||||||||
7476|Gogo Formation|32619|6|Mentioned|p464|||Givetian||||||
7476|Gogo Formation|32640|6|Mentioned|p237|||||||||
7476|Gogo Formation|32647|6|Mentioned|Fig. 24|||||||||
7476|Gogo Formation|32865|6|Mentioned|p473|||Frasnian||||||
7476|Gogo Formation|33042|6|Mentioned|p723|||Dev. Mentioned also on PP725-739, 742-753 etc.||||||
7476|Gogo Formation|34427|6|Mentioned|Fig.3|||||||||
7476|Gogo Formation|34484|6|Mentioned|p21|||||||||
7476|Gogo Formation|35104|6|Mentioned|p5|||||||||
7476|Gogo Formation|35526|6|Mentioned|p103|||||||||
7476|Gogo Formation|36225|6|Mentioned|Map legend|Frasnian|Givetian|Givetian to Frasnian||||||
7476|Gogo Formation|36365|6|Mentioned|Fig.8|||||||||
7476|Gogo Formation|36890|3|Fully described|p333|||||||||
7476|Gogo Formation|37319|6|Mentioned|p606|||||||||
7476|Gogo Formation|37751|6|Mentioned|p147|||||||||
7476|Gogo Formation|38207|4|Described|p162|||||||||
7476|Gogo Formation|38593|6|Mentioned|p87|||||||||
7476|Gogo Formation|39358|6|Mentioned|Fig.1|||||||||
7476|Gogo Formation|39702|6|Mentioned|Fig.2|||||||||
7476|Gogo Formation|40797|6|Mentioned|p155|||||||||
7476|Gogo Formation|40837|6|Mentioned|p264|||||||||
7476|Gogo Formation|40838|6|Mentioned|p279|||||||||
7476|Gogo Formation|40866|6|Mentioned|p180|||||||||
7476|Gogo Formation|40995|6|Mentioned|p395|||||||||
7476|Gogo Formation|41077|6|Mentioned|p203|||||||||
7476|Gogo Formation|41111|6|Mentioned|Fig.4|||||||||
7476|Gogo Formation|41113|6|Mentioned|p515|||||||||
7476|Gogo Formation|41139|6|Mentioned|Fig.2|||||||||
7476|Gogo Formation|41169|6|Mentioned|Fig.3|||||||||
7476|Gogo Formation|41215|6|Mentioned|Fig.4|||||||||
7476|Gogo Formation|41276|6|Mentioned|p69|||||||||
7476|Gogo Formation|41430|6|Mentioned|p18|||||||||
7476|Gogo Formation|41492|5|Briefly described|p114|||||||||
7476|Gogo Formation|41583|5|Briefly described|p21|||||||||
7476|Gogo Formation|41730|6|Mentioned|p472|||||||||
7476|Gogo Formation|41894|5|Briefly described|p4|||||||||
7476|Gogo Formation|42030|5|Briefly described|p747|||||||||
7476|Gogo Formation|42073|6|Mentioned|Fig.2 P292|||||||||
7476|Gogo Formation|42080|6|Mentioned|p281|||||||||
7476|Gogo Formation|42103|6|Mentioned|Fig.6 P257|||||||||
7476|Gogo Formation|42111|5|Briefly described|p88|||||||||
7476|Gogo Formation|42176|6|Mentioned|p204|||See also Fig.2||||||
7476|Gogo Formation|42347|6|Mentioned|Fig.2 P1020|||||||||
7476|Gogo Formation|42351|5|Briefly described|Fig.4 P41|||||||||
7476|Gogo Formation|42473|5|Briefly described|p4|||||||||
7476|Gogo Formation|42477|5|Briefly described|p102|||||||||
7476|Gogo Formation|42564|4|Described|p8|||||||||
7476|Gogo Formation|42582|6|Mentioned|p51|Late Devonian||||||||
7476|Gogo Formation|42860|5|Briefly described|Fig.2|||||||||
7476|Gogo Formation|42880|5|Briefly described|Fig.2,p1020|||||||||
7476|Gogo Formation|42933|5|Briefly described|Fig.94 p258|||||||||
7476|Gogo Formation|43173|6|Mentioned|54||Late Devonian|||||||
7476|Gogo Formation|43563|6|Mentioned|Fig.5,p10|Late Devonian|Middle Devonian|||||||
7476|Gogo Formation|43666|6|Mentioned|p47,Table 2|Frasnian|Givetian|||||||
7476|Gogo Formation|43723|6|Mentioned|p51||Devonian|||||||
7476|Gogo Formation|43786|6|Mentioned|p41||Devonian|||||||
7476|Gogo Formation|43825|6|Mentioned|p144||Frasnian|Source rock||||||
7476|Gogo Formation|44143|4|Described|p439 Table 4-19, p442, p443|Devonian|Devonian|Up to 650m thick; shale, siltstone and limestone; shallow marine. Interfingers with Sadler Limestone. Type section near Menyous Gap in Pillara Range (NOONKANBAH: 18deg 36' S, 125deg 26' E). Diverse fauna: late Givetian to early Frasnian. Spectacular fish fauna.||||||23-NOV-17
7476|Gogo Formation|44231|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Basin facies - siltstone, shale and calcarenite commonly with cannonball concretions; lesser sandstone and minor conglomerate.||||||18-MAY-05
7476|Gogo Formation|44397|14|Not recorded|p.12, Figs2,3,Table4|||Frasnian to (?) Givetian.||||||
7476|Gogo Formation|44398|14|Not recorded|map legend|||Frasnian to Givetian.||||||
7476|Gogo Formation|44403|2|Defined|opp.p.6,Tb.1|||E/51-12, limestone, siltstone, concretions. Overlain conformably by Virgin Hills Formation Underlain conformably by the Sadler Formation.||||||13-NOV-07
7476|Gogo Formation|44447|6|Mentioned|p135||Frasnian|||||||
7476|Gogo Formation|44998|14|Not recorded|p.26,36-7,41|||Interfingers with Sadler Formation.||||||
7476|Gogo Formation|45039|6|Mentioned|Fig.5|||Correlation.||||||
7476|Gogo Formation|45041|6|Mentioned|Fig.45|||||||||
7476|Gogo Formation|45063|6|Mentioned|Fig. 9|||Devonian||||||
7476|Gogo Formation|45101|4|Described|p6|||Conodont content. See also p21.||||||13-NOV-07
7476|Gogo Formation|45133|6|Mentioned|p4|||||||||
7476|Gogo Formation|45153|2|Defined|App.3-39|Frasnian|Frasnian|See also App.2-28||||||
7476|Gogo Formation|45158|3|Fully described|p26|||||||||
7476|Gogo Formation|46851|6|Mentioned|p217|||||||||
7476|Gogo Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
7476|Gogo Formation|47050|6|Mentioned|p244|||||||||
7476|Gogo Formation|48831|14|Not recorded|p.83,84,85|||||||||
7476|Gogo Formation|48837|2|Defined|p.28||Late Devonian|On many pages. p.18,25,26-28,39. Upper Devonian.||||||
7476|Gogo Formation|48848|14|Not recorded|p.94|||||||||
7476|Gogo Formation|48925|6|Mentioned|p100|||Upper Devonian age. Fauna||||||
7476|Gogo Formation|50077|6|Mentioned|p19|Frasnian|Frasnian|||||||
7476|Gogo Formation|50085|5|Briefly described|p6 Fig. 4|Devonian|Devonian|Of Frasnian age.  Geological Province: Canning Basin.||||||
7476|Gogo Formation|60333|4|Described|p801, 802|Frasnian|Givetian|Deposited within and around Sadler Limestone. Dark-grey to black shales and siltstones, with minor limestone lenses and bedded silty calcareous nodules. Contains various marine fossils (including a eurypterid described here). Geol. Prov: Canning Basin.||||||
7476|Gogo Formation|60702|5|Briefly described|p4|Frasnian|Frasnian|Thick, marine organic-rich shales.  - the source of oil for the Blina Field.   Geological Province: Canning Basin.||||||
7476|Gogo Formation|61023|5|Briefly described|p10 Fig. 6|Devonian|Devonian|Geological Province: Canning Basin. See also p12.||||||11-APR-08
7476|Gogo Formation|61551|6|Mentioned|p355, p359, p361. |Upper Devonian|Upper Devonian|Canning Basin. Hydrocarbon source rocks for suprasalt plays. Considered the most likely source rock for the Blina field.||||||
7476|Gogo Formation|63110|6|Mentioned|p1139|||Impermeable unit.||||||11-JUN-08
7476|Gogo Formation|63594|5|Briefly described|p1031|Frasnian|Frasnian|Contains Onychodus jandemarrai (Andrews et al, 2006) in Western Australia.||||||
7476|Gogo Formation|63738|6|Mentioned|p8|Visean|Visean|Contains actinopterygians.||||||
7476|Gogo Formation|63938|5|Briefly described|p49 Fig.1, p50 Fig.2|Frasnian|Givetian|Basin facies.||||||10-NOV-08
7476|Gogo Formation|64159|5|Briefly described|p91 Fig. 6|Frasnian|Givetian|Part of the Lennard Reef facies development. Mainly a siltstone unit.||||||
7476|Gogo Formation|64187|5|Briefly described|p320 Fig. 2|Frasnian|Frasnian|Overlain by Virgin Hills Formation. Siltstone, sandstone, carbonate (marine). Geological Province: Canning Basin.||||||01-MAY-13
7476|Gogo Formation|64348|6|Mentioned|p393, p406|Frasnian|Frasnian|Contains fossil actinopterygian fish of exceptional quality.||||||
7476|Gogo Formation|64502|5|Briefly described|p764, p765 Fig. 2|Frasnian|Givetian|||||||27-JAN-10
7476|Gogo Formation|64580|5|Briefly described|map legend|||Givetian-Frasnian reef complexes, marginal slope and basin facies.||||||15-DEC-08
7476|Gogo Formation|64643|5|Briefly described|p5 Fig. 4, p7 Fig.5, p34, 35|Frasnian|Givetian|Basin facies.||||||17-NOV-08
7476|Gogo Formation|64783|6|Mentioned|p101|||Canning Basin.||||||15-NOV-17
7476|Gogo Formation|64981|5|Briefly described|p672.|Frasnian|Givetian|Generally-accepted source of both Nullara and Yellow Drum Formations oil.|||||Shales containing marine algae deposited in an anoxic environment.|
7476|Gogo Formation|65214|6|Mentioned|p277|Devonian|Devonian|QLD, Broken River and Canning Basin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
7476|Gogo Formation|65486|5|Briefly described|p6-7,9,48-50; Figs.5,6,7,67; Plate 1.|Frasnian|Givetian|Marginal-slope and basin limestone, siltstone, and shale, Canning Basin. Overlies Cadjebut Formation, Pillara Limestone. Overlies and interfingers with Sadler Limestone. Underlies Napier and Virgin Hills Formations.||||||
7476|Gogo Formation|66127|3|Fully described|p19-21, p51-54, p184-206, Pl. 3,4,5,7,8.|Early Frasnian|Late Givetian|Of Guppy et al. (1958), after Gogo Station. Type section is SE of the northern entrance to Menyous Gap. Each facies mapped separately. Poorly exposed. Limestone concretions ("Gogo nodules") common where unit abuts Sadler Limestone. Fossiliferous. Thickness to 700 m. Contains stromatolite-barite-sulfide exhalative deposits.||||Locally overlies Pillara Limestone. Interfingers with and overlies Sadler Limestone. Locally interfingers with Sparke Conglomerate. Is overlain conformably by Virgin Hills Formation.|Grey to black shales and siltstone; thin limestones from debris-flows and turbidity currents. Basin facies and lower fore-reef subfacies; grey, weathering yellow, siltstone, shale and silty limestone.|
7476|Gogo Formation|66499|5|Briefly described|p62, p63 Fig.7|||Has yielded the most diverse and exceptionally preserved of the world's Late Devonian marine fish faunas. Fauna said to be of Frasnian age.||||||
7476|Gogo Formation|67131|6|Mentioned|p3 Fig. 2,|Frasnian|Givetian|Basin facies.||||Overlain by Virgin Hills Formation.||
7476|Gogo Formation|68297|6|Mentioned|p193|Frasnian|Frasnian|Canning Basin.||||||
7476|Gogo Formation|68298|5|Briefly described|p219,  p249 App. 1||Late Devonian|Late Devonian diverse and well-studied fauna of the Canning Basin.||||||
7476|Gogo Formation|69029|5|Briefly described|p313,321,333|Devonian|Devonian|Of Canning Basin. Inter-reef complex deposited during major Frasnian transgression. Shale contain up to 3% TOC (Ellyard, 1984). Source rocks generated oils to the Blina Oilfield.||||Overlain by Fairfield Group.||
7476|Gogo Formation|69099|5|Briefly described|500k_geologyp08_lut.csv|Frasnian|Givetian|Givetian-Frasnian reef complexes, marginal slope and basin facies. Grouped as Sadler Limestone, Gogo Formation, lower Virgin Hills Formation, and lower Napier Formation in 500k_geologyp08_lut.csv.||||||
7476|Gogo Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Givetian|||||||
7476|Gogo Formation|69182|6|Mentioned|Ch4 p87|||||||||
7476|Gogo Formation|69206|6|Mentioned|p2|Devonian|Devonian|Canning Basin. Source of oil in the Blina field.||||||
7476|Gogo Formation|69297|6|Mentioned|p354|Lower Carboniferous|Upper Devonian|Canning Basin. Contains good potential oil source rocks. ||||||
7476|Gogo Formation|69312|6|Mentioned|p1, p3, p9, p23 fig 27|Frasnian|Frasnian|Canning Basin. Contains oil-prone source rocks and has a TOC of up to 4 percent. One of the three petroleum systems that forms the Larapintine Petroleum Supersystem. See also p26 fig 33, p29, p30, p31. ||Pillara Sequence||Overlies the Tandalgoo Sandstone.||
7476|Gogo Formation|70272|6|Mentioned|p879 Fig.3|||||||||
7476|Gogo Formation|71146|6|Mentioned|p32|Devonian|Devonian|Canning Basin. Deposited as the basin facies of the devonian reef complex in the basin. This unit contains well preserved fossil verterbrates and inverterbrates.||||||
7476|Gogo Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fossiliferous shallow marine reef complex basin facies black to light grey shale and siltstone with thin lenses of limestone and layers with abundant limestone concretions|
7476|Gogo Formation|71870|6|Mentioned|p1|Upper Devonian|Upper Devonian|Canning Basin. A petroleum source interval formed during the Larapintine petroleum supersystem.||||||
7476|Gogo Formation|72502|6|Mentioned|p5|Frasnian|Givetian|Lennard Shelf, Canning Basin.||||Underlain by Cadjebut Formation. Overlain by Virgin Hills Formation. Equivalent to Napier Formation and Sadler Limestone.||
7476|Gogo Formation|73117|6|Mentioned|p32|Famennian|Frasnian|Hydrocarbon source interval.||||||
7489|Golden Bar Sill|42221|6|Mentioned|Table 1 P6|||||||||
7489|Golden Bar Sill|42892|5|Briefly described|Fig.27, Table 5|||of Coolgardie Group||||||
7489|Golden Bar Sill|43162|6|Mentioned|5|||||||||
7489|Golden Bar Sill|43496|6|Mentioned|6-15|||||||||
7489|Golden Bar Sill|60627|5|Briefly described|p65 Tb.1|||Of Coolgardie Group.||||||
7489|Golden Bar Sill|65834|6|Mentioned|p7|||Coolgardie Domain, Kalgoorlie Terrane.||Coolgardie Group.||||
7489|Golden Bar Sill|73391|6|Mentioned|Appendices.|||Hunter (1993). Regional stratigraphic correlation chart of other workers.|||||Dolerite.|
7497|Golden Gate Siltstone|22547|4|Described|p24|Stenian|Ectasian|Of the Carr Boyd Group. Geological province: Carr Boyd Basin. Age: 1158 +/- 123 Ma. Thickness: 60 m. Overlies Hensman Sandstone, overlain by Lissadell Formation.||||||14-NOV-06
7497|Golden Gate Siltstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group||||||
7497|Golden Gate Siltstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
7497|Golden Gate Siltstone|32660|5|Briefly described|Table 6|||||||||
7497|Golden Gate Siltstone|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
7497|Golden Gate Siltstone|32728|5|Briefly described|Table 6|||See also P46||||||
7497|Golden Gate Siltstone|33443|6|Mentioned|p261|||||||||
7497|Golden Gate Siltstone|36551|6|Mentioned|Table 12|||||||||
7497|Golden Gate Siltstone|36885|4|Described|p179|||||||||
7497|Golden Gate Siltstone|37462|6|Mentioned|Fig.4.13|||||||||
7497|Golden Gate Siltstone|40765|6|Mentioned|p11|||||||||
7497|Golden Gate Siltstone|40813|6|Mentioned|p335|||||||||
7497|Golden Gate Siltstone|41158|5|Briefly described|p39|||Of the Carr Boyd Group. Overlies Hensman Sandstone. Mention p19.||||||28-SEP-06
7497|Golden Gate Siltstone|42191|5|Briefly described|Fig.7 P140|||||||||
7497|Golden Gate Siltstone|43853|5|Briefly described|Map Legend||Proterozoic|||||||
7497|Golden Gate Siltstone|44155|5|Briefly described|p250 Tb.3-10|||240 - 2000m thick. Facies change and thickness increases progressively from west to east.||Carr Boyd Group|||Lithic subgreywacke, red and green micaceous shale, hematitic sandstone in west; black (pyritic) siltstone and shale with blocky sandstone in east.|
7497|Golden Gate Siltstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
7497|Golden Gate Siltstone|44363|4|Described|p.6,14,15,16-7,23-28|||(Adelaidean). Of Carr Boyd Group.||||||28-SEP-06
7497|Golden Gate Siltstone|44364|14|Not recorded|map legend||Proterozoic|||||||
7497|Golden Gate Siltstone|45047|4|Described|p35|||Of Carr Boyd Group.||||||28-SEP-06
7497|Golden Gate Siltstone|45112|6|Mentioned|Table 16|||||||||
7497|Golden Gate Siltstone|48938|6|Mentioned|p76|||Refers Dow & Gemuts.||||||
7497|Golden Gate Siltstone|65417|5|Briefly described|pp156-159.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Age from Bofinger (1967) recalculated by Plumb et al. (1981). Transgressive offshore shelf deposits.|1158 +/- 123 Ma (Rb-Sr whole rock).|Unit in Carr Boyd Group.||Conformably overlies Hensman Sandstone. Is overlain conformably by Lissadell Formation.||
7497|Golden Gate Siltstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin||Carr Boyd Group|||Siltstone and mudstone; carbonaceous, chloritic or micaceous; thin- to medium-bedded ferruginous sandstone and quartz sandstone.|31-JUL-15
7497|Golden Gate Siltstone|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Siltstone and mudstone, either carbonaceous, chloritic or micaceous; thin to medium-bedded dolomitic sandstone, siltstone, mudstone and stromatolitic chert.|
7497|Golden Gate Siltstone|69435|5|Briefly described|p20:3|||Carr Boyd Basin.||Carr Boyd Group.||Overlies Hensman Sandstone. Is overlain by Lissadell Formation.||12-JUL-16
7497|Golden Gate Siltstone|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1200-1177 Ma (Inferred)|Unit of Carr Boyd Group.|||Siltstone and mudstone; carbonaceous, chloritic or micaceous; thin- to medium-bedded ferruginous sandstone and quartz sandstone|
7497|Golden Gate Siltstone|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Lissadell Formation, overlies Hensman Sandstone||
7497|Golden Gate Siltstone|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1177-1200 Ma|Carr Boyd Group|||Siltstone and mudstone, carbonaceous, chloritic or micaceous; thin to medium bedded ferruginous sandstone and quartz sandstone.|
7497|Golden Gate Siltstone|70812|5|Briefly described|p23|Middle Proterozoic|Middle Proterozoic|||||||
7497|Golden Gate Siltstone|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1200-1177 Ma (inferred)|Unit of Carr Boyd Group.|||Siltstone and mudstone; carbonaceous, chloritic or micaceous; thin- to medium-bedded ferruginous sandstone and quartz sandstone|
7505|Golden Ridge porphyry|41249|6|Mentioned|p39|||||||||
7530|Goobaieri Formation|22547|6|Mentioned|Fig4,p25|||Of Fitzmaurice Group. Overlies Moyle River Formation.||||||14-NOV-06
7530|Goobaieri Formation|32307|4|Described|Table 2|||Proterozoic||||||
7530|Goobaieri Formation|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
7530|Goobaieri Formation|32660|5|Briefly described|Table 6|||||||||
7530|Goobaieri Formation|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Fitzmaurice Group.  Quartz sandstone overlain by siltstone and sandstone.||||||02-DEC-04
7530|Goobaieri Formation|32701|4|Described|Table 1|||Adelaidean. Of the Fitzmaurice Group.||||||21-SEP-06
7530|Goobaieri Formation|32728|6|Mentioned|Fig.14|||||||||
7530|Goobaieri Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
7530|Goobaieri Formation|37462|6|Mentioned|Fig.4.13|||||||||
7530|Goobaieri Formation|40494|6|Mentioned|p10|||||||||
7530|Goobaieri Formation|40765|6|Mentioned|p11|||||||||
7530|Goobaieri Formation|41645|4|Described|p16|||||||||
7530|Goobaieri Formation|41646|6|Mentioned|Map legend|Mesoproterozoic||Of the Fitzmaurice Group. Siltstone; interbedded fine grained quartzarenite.||||||17-OCT-05
7530|Goobaieri Formation|45112|6|Mentioned|Table 16|||||||||
7530|Goobaieri Formation|48938|2|Defined|p15|Adelaidean|Adelaidean|Measured section p88.||||||21-SEP-06
7530|Goobaieri Formation|48942|3|Fully described|p34|||Strat. sections pp108,109.||||||21-SEP-06
7530|Goobaieri Formation|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: ? Halls Creek Orogen. Of Fitzmaurice Group. Quartz sandstone, shale, siltstone.||||||19-JUL-04
7530|Goobaieri Formation|60682|4|Described|p5|Mesoproterozoic|Mesoproterozoic|Of Fitzmaurice Group. Thickness: >615m. Conformably overlies Moyle River Formation. Conformably/disconformably overlain by Lalngang Sandstone. Geological Province: Halls Creek Orogen.||||||
7530|Goobaieri Formation|64698|4|Described|lithinterp table|||Age stated to be ~1150-1250Ma (Stenian), but age name given is Statherian? Victoria - Birrindudu Basin. Of Fitzmaurice Group. Max thickness 700m. Quartz sandstone, shale, siltstone. Conformably overlies Moyle River Formation.||||||07-JAN-09
7530|Goobaieri Formation|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Fitzmaurice Group, ?Halls Creek Orogen. Quartz sandstone, shale, siltstone ||||||
7530|Goobaieri Formation|65417|5|Briefly described|p158 Fig.2.|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Mobile Zone.||Unit in Fitzmaurice Group.||Conformably overlies Moyle River Formation.||
7530|Goobaieri Formation|67167|5|Briefly described|Map legend.|||||Unit in Fitzmaurice Group.|||Quartz sandstone, shale, siltstone.|
7530|Goobaieri Formation|69435|4|Described|p20:2-4, 6|||Sweet et al. (1974). Fitzmaurice Basin. No accurate measure of thickness; varies from 0 to 600m.||Fitzmaurice Group.||Conformably overlies Moyle River Formation. Is overlain by Lalngang Sandstone conformably (?regionally disconformably).|Fissile siltstone, shale and medium- to fine-grained sandstone. Shows wide lateral facies variation. Cross-beds and ripple marks are present locally.|12-JUL-16
7530|Goobaieri Formation|69673|5|Briefly described|p59, p60 fig 48|||||Fitzmaurice Group||Overlain by Lalngang Sandstone, overlies Moyle River Formation|Siltstone, shale and medium to fine grained sandstone with a  maximum thickness in excess of 600m.|
7530|Goobaieri Formation|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Fitzmaurice Basin.||Fitzmaurice Group|||Quartz sandstone, shale and siltstone.|
7530|Goobaieri Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
7555|Googhenama Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
7555|Googhenama Formation|23590|3|Fully described|p11|||Of Tarcunyah Group. Overlying unit Waroongunyah Formation. Geological Province: Officer Basin. Max. thickness ~400 m.||||||
7555|Googhenama Formation|23594|4|Described|p21|Neoproterozoic|Mesoproterozoic|Previously mapped as Bocrabee Sandstone (Hickman, 1978). Of Tarcunyah Group. Overlain by Waroongunyah Formation. Underlain by Gregory Granitic Complex. Bangemall Basin.||||||24-JUL-07
7555|Googhenama Formation|23745|4|Described|p17|Neoproterozoic|Mesoproterozoic|See also page 7 Fig 5. Of Tarcunyah Group. Yeneena Basin. Max. thickness: 700 m.||||||
7555|Googhenama Formation|23746|4|Described|p25|Neoproterozoic|Mesoproterozoic|Formerly Bocrabee Sandstone. Of Tarcunyah Group.||||||
7555|Googhenama Formation|23760|4|Described|p26|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
7555|Googhenama Formation|24025|5|Briefly described|p16|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Geological Province: Officer Basin.||||||
7555|Googhenama Formation|42352|5|Briefly described|p7|||Formerly Bocrabee Sandstone and Googhenama Conglomerate. Part of Yeneena Group.||||||
7555|Googhenama Formation|43055|4|Described|p27, Table 4|||of Yeneena Group||||||
7555|Googhenama Formation|43847|5|Briefly described|Map Legend||Proterozoic|||||||17-FEB-10
7555|Googhenama Formation|44111|6|Mentioned|p58.|||Basal unit in Tarcunyah Group. Is lithologically similar to Coondra Formation (Savory Basin) and Townsend Quartzite (Officer Basin).||||||
7555|Googhenama Formation|44139|5|Briefly described|p277-279, p282|||Basal unit in western zone of Yeneena Basin (Williams 1989). Originally the Googhenama Conglomerate. Overlain by Waroongunyah Formation. Incorporates former Bocrabee Sandstone rocks. 0-250 m. Sandstone, cobble conglomerate. Fluviatile or near-shore shallow-marine.| | ||||05-MAR-18
7555|Googhenama Formation|44152|6|Mentioned|p176 Fig.2-154, p177|||||Yeneena Group||||
7555|Googhenama Formation|44189|5|Briefly described|Map legend||Proterozoic|||||||
7555|Googhenama Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
7555|Googhenama Formation|44831|5|Briefly described|Map Legend||Proterozoic|||||||
7555|Googhenama Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Tarcunyah Group. Geological Province: Officer Basin.||||||
7555|Googhenama Formation|50544|4|Described|p58|Neoproterozoic|Neoproterozoic|Basal unit of the Tarcunyah Group.  Mixed sandstone.  Max. thickness: 300m.  Overlain by Waroongunyah Fm; unconformably overlies Gregory Granitic Complex, the Koongaling Volcanic and Warroo Hill Members (of the Hardey Fm) and the Kylena Fm (Fortescue Gp).||||||
7555|Googhenama Formation|50555|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Medium to coarse-grained sandstone, quartz wacke, and thin beds of pebble to cobble conglomerate.  Geological Province: Officer Basin.||||||23-DEC-09
7555|Googhenama Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Sandstone; minor conglomerate, siltstone, and shale||||||
7555|Googhenama Formation|62453|3|Fully described|p5 Fig. 3, 63|Cryogenian|Tonian|Geological Province: Paterson Orogen. Of the Tarcunyah Group. Includes former Bocrabee Sandstone. Thickness: ~500m. Sandstone, conglomerate. ||||||
7555|Googhenama Formation|63417|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Geological Province: Officer Basin (Centralia Superbasin). Sandstone and granule to pebble conglomerate.||||||23-JUL-07
7555|Googhenama Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
7555|Googhenama Formation|64777|5|Briefly described|p3 Fig.4|Neoproterozoic|Neoproterozoic|||Of the Tarcunyah Group|||Sandstone; minor conglomerate, siltstone and shale|
7555|Googhenama Formation|65454|4|Described|p7 Fig.3, p10, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Interbedded fine- to coarse-grained sandstone and granular to pebbly conglomerate. Unconformably overlies Archean basement. Overlain by Waroongunyah Formation.||||||
7555|Googhenama Formation|65725|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Tarcunyah Group. Overlain by Waroongunyah Formation. Medium- to coarse-grained sandstone and pebble to boulder conglomerate. Province: Officer Basin (Centralian Superbasin)||||||26-FEB-13
7555|Googhenama Formation|65826|4|Described|p1, pp10-11. |Neoproterozoic|Neoproterozoic|Fluviatile succession. Up to 500m thick.||Basal unit in Tarcunyah Group.||Is overlain conformably by Waroongunyah Formation.|Interbedded fine- to coarse-grained, light pink to purple coloured sandstone, commonly quartz-rich with ripple marks; granular to boulder conglomerate, lenticular, commonly matrix-supported, quartz-pebble rich or polymictic.|23-MAY-16
7555|Googhenama Formation|67183|5|Briefly described|p645, p665, p666 Fig.25, p671 |Neoproterozoic|Neoproterozoic|Basal Tarcunyah Group in the Officer Basin. Mis-spelt as Googenhama Conglomerate (Fig.25) and as Googenhama Formation (p648, p649 Fig.8, p651 Fig.10).|ca 850 Ma|Tarcunyah Group||Unconformably overlies the Manganese Subgroup.|Boulder to pebble conglomerate that grades up to a medium-grained sandstone. In the Fig Tree prospect consists of matrix supported, polymictic to quartz pebble-rich conglomerate. Trough cross-bedding and ripples.|
7555|Googhenama Formation|67202|4|Described|p64-65, p117, p125, p231-237, p273, p278|Neoproterozoic|Neoproterozoic|NW Officer Basin. Braided stream deposits. 500m thick. Crops out as a 50km-long, almost continuous ridge. Conductance image. Locally-derived granitic and gneissic clasts are a good source of uranium.||Basal Tarcunyah Group.||Unconformably overlies Fortescue Group, Gregory Granite Complex and Woblegun Formation. Is overlain conformably by Waroongunyah Formation. Is faulted against the Broadhurst Formation.|Mixed medium- to coarse-grained sandstone and pebble to boulder conglomerate sequence.|
7555|Googhenama Formation|67430|6|Mentioned|p22|||Paterson Province.||||||
7555|Googhenama Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
7555|Googhenama Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Tarcunyah Group|||Sandstone and granule to pebble conglomerate.|
7555|Googhenama Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
7555|Googhenama Formation|69590|4|Described|GEOL_LUT_CSV files|Cryogenian|Neoproterozoic|Of Gibson Sub-basin, Officer Basin (Phase 1), Centralian Superbasin. Events: Delamarian Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1000-635 Ma (Inferred)|Unit of Tarcunyah Group.|||Granule to pebble conglomerate interbedded with fine- to coarse-grained sandstone|
7555|Googhenama Formation|71042|5|Briefly described|p67, p71, p74|||Officer Basin. See also Googenhama Formation [which is a mis-spelling of this unit].|ca 850 Ma|Tarcunyah Group||Unconformably overlies the Manganese Group, Carawine Dolomite and Pinjian Chert Breccia. Overlies the Jeerinah and Maddina Formations.|Conglomerate.|
7555|Googhenama Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
7555|Googhenama Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Granule to pebble conglomerate interbedded with fine- to coarse-grained sandstone.|
7569|Goongarrie Monzogranite|22534|4|Described|p11|||||||||
7569|Goongarrie Monzogranite|22539|5|Briefly described|Map legend|Archean|Archean|||||||07-NOV-08
7569|Goongarrie Monzogranite|22841|5|Briefly described|Map legend||Archean|||||||07-NOV-08
7569|Goongarrie Monzogranite|22890|6|Mentioned|P13|||||||||
7569|Goongarrie Monzogranite|41786|5|Briefly described|p336|||Reserved as Goongarrie Adamellite||||||
7569|Goongarrie Monzogranite|42382|4|Described|p37|||||||||
7569|Goongarrie Monzogranite|42705|5|Briefly described|map legend|Archean||||||||07-NOV-08
7569|Goongarrie Monzogranite|42742|5|Briefly described|map legend|Archean||||||||07-NOV-08
7569|Goongarrie Monzogranite|42988|5|Briefly described|Map Legend|||||||||
7569|Goongarrie Monzogranite|42989|5|Briefly described|p12|||||||||
7569|Goongarrie Monzogranite|43074|5|Briefly described|p17|||||||||
7569|Goongarrie Monzogranite|43101|5|Briefly described|p26|||||||||
7569|Goongarrie Monzogranite|43214|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
7569|Goongarrie Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
7569|Goongarrie Monzogranite|50075|5|Briefly described|p17|Archean|Archean|Geological Province: Yilgarn Craton.||||||23-DEC-09
7569|Goongarrie Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite monzogranite.  Geological Province: Yilgarn Craton.||||||23-DEC-09
7569|Goongarrie Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmgo]  Locally K-feldspar-phyric, biotite-bearing; weak to moderate foliation; deformed contacts.||||||02-FEB-05
7569|Goongarrie Monzogranite|65204|6|Mentioned|p17 Tbl.2.|Neoarchean||0.4-10mm grains; seriate to porphyritic ||||||
7569|Goongarrie Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Biotite-bearing monzogranite with local prominent K-feldspar megacrysts; weak to moderate foliation; deformed contacts.||||||07-FEB-11
7569|Goongarrie Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Biotite-bearing monzogranite with local prominent K-feldspar megacrysts; domal within D2 anticline; weak to moderate foliation; deformed contacts.|06-AUG-15
7569|Goongarrie Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Biotite-bearing monzogranite with local prominent K-feldspar megacrysts; domal within D2 anticline; weak to moderate foliation; deformed contacts.|
7569|Goongarrie Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
7569|Goongarrie Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Biotite-bearing monzogranite with local prominent K-feldspar megacrysts; domal within D2 anticline; weak to moderate foliation; deformed contacts|
7646|Goyder Formation|9199|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Silty sandstone, siltstone, limestone, dolomite.  Geological Province: Amadeus Basin.||||||04-NOV-04
7646|Goyder Formation|9814|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Sandstone, limestone, siltstone; fossiliferous.||||||
7646|Goyder Formation|12891|5|Briefly described|p732|Late Cambrian|Late Cambrian|Geological province: Amadeus Basin. Lithology possibly analogous with Point Wakefield beds in Wiso Basin.||||||07-FEB-11
7646|Goyder Formation|22560|6|Mentioned| p5|||||||||
7646|Goyder Formation|22561|4|Described|p21|Late Cambrian|Neoproterozoic|Includes sequence boundary between the lower and upper Goyder Formation, which marks a significant change in depositional patterns within the basin.||||||06-FEB-08
7646|Goyder Formation|22565|5|Briefly described|p71 & Table 1||Cambrian|Thickness at Areyonga Creek measured from surface expression - 330m thick.  Approx. thickness measured from seismic data - 350m.||||||
7646|Goyder Formation|22566|5|Briefly described|p84|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22646|5|Briefly described|p 104|Cambrian|Cambrian|informally devided into upper and lower Goyder Formation p 104.||||||13-SEP-18
7646|Goyder Formation|22650|5|Briefly described|p 160|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22651|4|Described|p 188|Late Cambrian|Middle Cambrian|Of Pertaoorrta Group. Informally devided into upper and lower Goyder Formation p171. The upper Goyder Formation contains late Cambrian trilobites, this suggests a significant time break between it and the lower Goyder which contains Mindyallan fauna.||||||21-SEP-06
7646|Goyder Formation|22655|6|Mentioned|p 253|||informally devided into upper and lower Goyder Formation p255.||||||
7646|Goyder Formation|22656|6|Mentioned|Fig 5 on p 283|||||||||
7646|Goyder Formation|22657|5|Briefly described|p 285|||Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22758|6|Mentioned|Fig 2 on p305|||||||||
7646|Goyder Formation|22760|6|Mentioned|p337|||||||||
7646|Goyder Formation|22762|6|Mentioned|p364|Cambrian|Cambrian|||||||
7646|Goyder Formation|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22804|6|Mentioned|p429|Early Ordovician|Cambrian|Of Pertaoorrta Group.  Informally devided into upper and lower Goyder Formation.||||||21-SEP-06
7646|Goyder Formation|22805|5|Briefly described|p470||Late Cambrian|||||||
7646|Goyder Formation|22807|6|Mentioned|p500|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22824|5|Briefly described|p533|||Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|22826|4|Described|p572|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|24064|5|Briefly described|p229 Fig.7|Cambrian|Cambrian|Of Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|29591|5|Briefly described|Table 23|||||||||
7646|Goyder Formation|29721|6|Mentioned|Table 44|||||||||
7646|Goyder Formation|29972|6|Mentioned|Table 1|||Upper Cambrian||||||
7646|Goyder Formation|30258|6|Mentioned|Fig.2|||Cambrian age.  Part of Pertaoorta Group.||||||21-SEP-06
7646|Goyder Formation|30544|6|Mentioned|p48|||||||||
7646|Goyder Formation|31572|6|Mentioned|p21|||U.Cambrian. Correlation chart 1.||||||
7646|Goyder Formation|32469|6|Mentioned|p531|||||||||
7646|Goyder Formation|33307|6|Mentioned|Fig.6|||||||||
7646|Goyder Formation|33625|6|Mentioned|p189|||||||||
7646|Goyder Formation|33738|6|Mentioned|p47|||||||||
7646|Goyder Formation|33761|6|Mentioned|p146|||Cambrian||||||
7646|Goyder Formation|34111|5|Briefly described|Table 2|||Cambrian. See also pp6,15,20.||||||21-SEP-06
7646|Goyder Formation|34186|6|Mentioned|p1988|||Upper Cambrian. See also Figs.3,4,8.||||||
7646|Goyder Formation|34442|5|Briefly described|Table 1|||Camb. p8||||||21-SEP-06
7646|Goyder Formation|34579|4|Described|Table 2|||Cambrian. See also pp16,17.||||||21-SEP-06
7646|Goyder Formation|35102|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|35805|6|Mentioned|Fig.3|||||||||
7646|Goyder Formation|36198|6|Mentioned|p295|||See also Fig.III.2||||||
7646|Goyder Formation|38606|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7646|Goyder Formation|38885|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7646|Goyder Formation|39210|5|Briefly described|p38|||||||||
7646|Goyder Formation|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
7646|Goyder Formation|39583|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
7646|Goyder Formation|39757|6|Mentioned|p1607|||||||||
7646|Goyder Formation|39931|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
7646|Goyder Formation|40136|6|Mentioned|p36|||||||||
7646|Goyder Formation|40740|3|Fully described|p44|||Mention p5.||||||21-SEP-06
7646|Goyder Formation|40810|4|Described|p7|||||||||
7646|Goyder Formation|40852|6|Mentioned|p34|||||||||
7646|Goyder Formation|40906|6|Mentioned|Fig.11|||||||||
7646|Goyder Formation|40998|6|Mentioned|Fig.1|||||||||
7646|Goyder Formation|41018|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41115|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41190|6|Mentioned|Fig.4|||||||||
7646|Goyder Formation|41203|5|Briefly described|p30|||||||||
7646|Goyder Formation|41224|6|Mentioned|p430|||||||||
7646|Goyder Formation|41621|5|Briefly described|Map legend|Cambrian||||||||
7646|Goyder Formation|41717|6|Mentioned|Fig.2|||||||||
7646|Goyder Formation|41723|6|Mentioned|Map legend|Neoproterozoic|Early Cambrian|||||||
7646|Goyder Formation|41819|6|Mentioned|Map legend|Cambrian||||||||
7646|Goyder Formation|41820|3|Fully described|p7|||||||||
7646|Goyder Formation|42037|5|Briefly described|Table 3 P79|||||||||
7646|Goyder Formation|42060|6|Mentioned|Fig.5 P140|||||||||
7646|Goyder Formation|42082|6|Mentioned|Fig.3 P323|||||||||
7646|Goyder Formation|42354|4|Described|p6|Late Cambrian||||||||
7646|Goyder Formation|42504|5|Briefly described|p112|||||||||
7646|Goyder Formation|42886|5|Briefly described|Fig.1 P218|||||||||
7646|Goyder Formation|42940|5|Briefly described|p1 Plate8|||||||||
7646|Goyder Formation|43225|5|Briefly described|Map Legend||Cambrian|Of Pertaoorrta Group.||||||21-SEP-06
7646|Goyder Formation|43503|6|Mentioned|11-50|Payntonian|Mindyallan|||||||
7646|Goyder Formation|43646|6|Mentioned|Fig.3,p554||Late Cambrian|||||||
7646|Goyder Formation|43648|6|Mentioned|Fig.27,p509|||||||||
7646|Goyder Formation|43649|6|Mentioned|p457|||||||||
7646|Goyder Formation|43781|6|Mentioned|p4|||||||||
7646|Goyder Formation|43807|5|Briefly described|p352|||||||||
7646|Goyder Formation|44395|14|Not recorded|p.8||Cambrian|Correlates with Cleland Sandstone.||||||
7646|Goyder Formation|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
7646|Goyder Formation|44433|14|Not recorded|map legend||Cambrian|||||||
7646|Goyder Formation|44457|14|Not recorded|p.6||Late Cambrian|Amadeus Basin. Upper Cambrian. (Mindyallan).||||||
7646|Goyder Formation|44484|14|Not recorded|p.10,14, Tb.1||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44485|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44497|4|Described|p.10, Table 1||Cambrian|SF/53-13.||||||
7646|Goyder Formation|44498|14|Not recorded|map legend||Cambrian|Part of Pertaoorrta Group.||||||
7646|Goyder Formation|44505|14|Not recorded|p.7,11,12, Table 1||Cambrian|Of Pertaoorrta Group.||||||
7646|Goyder Formation|44506|14|Not recorded|map legend||Cambrian|||||||
7646|Goyder Formation|45041|4|Described|p58|||Refers Prichard and Quinlan (1962). U.Camb.||||||21-SEP-06
7646|Goyder Formation|45115|6|Mentioned|p7|||||||||
7646|Goyder Formation|45130|6|Mentioned|p14|||||||||
7646|Goyder Formation|45148|6|Mentioned|Fig.4|||Amadeus Basin||||||
7646|Goyder Formation|45155|6|Mentioned|Fig.8|||||||||
7646|Goyder Formation|46826|5|Briefly described|p345|||||||||
7646|Goyder Formation|46928|6|Mentioned|Table 1|||||||||
7646|Goyder Formation|48639|14|Not recorded|p.5||Cambrian|See also page, 1,4,6,17,Pl.1,Sh.2.||||||
7646|Goyder Formation|48838|2|Defined|p.16, Tb.1||Late Cambrian|U.Cam.||||||
7646|Goyder Formation|48862|14|Not recorded|p.17|||Now superseded by Goyder Member. (F52-15).||||||
7646|Goyder Formation|48863|2|Defined|p.23||Late Cambrian|Tb.1. opp.p.7,p.5,9,14,16,19,20,24,25,33,43,Pl.10,11,15,16. Upper Cambrian. (G52-4,G53-1).||||||
7646|Goyder Formation|48865|14|Not recorded|Fig.4|||(G52-4,F53-13).||||||
7646|Goyder Formation|48890|4|Described|p.42||Cambrian|See also Tables, Figs, Plates. pt. Pertaoorta Gp.||||||
7646|Goyder Formation|48963|6|Mentioned|p30|||Fig.3||||||
7646|Goyder Formation|50246|5|Briefly described|p20 Fig. 2|Cambrian|Cambrian|Sandstone, limestone.||||||07-FEB-11
7646|Goyder Formation|60547|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Silty sandstone, siltstone, limestone, dolomite. Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Yellow-brown, partly micaceous, kaolinitic sandstone; minor stromatolitic limestone, oolitic dolostone and siltstone. Geological Province: Amadeus Basin.||||||13-SEP-18
7646|Goyder Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
7646|Goyder Formation|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, siltstone, calcareous.  Geological Province: Amadeus Basin.||||||
7646|Goyder Formation|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Yellow-brown, partly micaceous, kaolinitic sandstone; minor stromatolitic limestone, oolitic dolostone and siltstone. Geological Province: Amadeus Basin.||||||23-DEC-09
7646|Goyder Formation|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin. ||||||
7646|Goyder Formation|62379|4|Described|p13|Late Cambrian|Late Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin. Shale, siltstone, sandstone, limestone, dolostone.||||||
7646|Goyder Formation|62595|6|Mentioned|p28 Fig.4, p29 Fig.6.|Late Cambrian|Late Cambrian|Amadeus Basin. Relative probability plots of detrital zircon data are shown.|||||Sandstone, limestone.|
7646|Goyder Formation|62794|5|Briefly described|p289 Fig.2|Late Cambrian|Late Cambrian|Topmost unit of Pertaoorrta Group. Underlies Pacoota Sandstone of the Larapinta Group.||||||
7646|Goyder Formation|63562|4|Described|p338 fig 3, p340-341, p346-349|Late Cambrian|Late Cambrian|See also p352 fig 10, p355. Of Amadeus Basin. Zircons from lower part were mostly 1.2-0.9 Ga suggesting Musgrave Inlier as source. Also has a peak at 0.55 Ga with no apparent source other than the Lachlan Fold Belt, more than 1000 km to the E.||||Overlies Shannon Formation. Is overlain by Pacoota Sandstone.|Includes dolomite, calcarenite.|
7646|Goyder Formation|64068|6|Mentioned|p65, 67, 69, 70, 71, 225|||Amadeus Basin. Lower part correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone, southern Georgina Basin. Upper part correlated with Chatsworth Limestone. ||||||
7646|Goyder Formation|64334|6|Mentioned|p45|||Detrital zircon ages and provenances discussed.||||||
7646|Goyder Formation|64778|6|Mentioned|p13, 18, 21, 33|Cambrian|Cambrian|Amadeus Basin.||||||
7646|Goyder Formation|64809|4|Described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10.|Late Cambrian|Late Cambrian|See also p13 Fig.13, p15 Fig.15. Widespread transgressive deposits.||Unit in Pertaoorrta Group.|||Silty sandstone, limestone|
7646|Goyder Formation|65233|3|Fully described|p3 Fig. 2, p9|Late Cambrian|Late Cambrian|Of Pertaoorrta Gp. Gradationally related to clastic succession below. Max.thick: 600m. Amadeus Basin. Basal carbonate-clastic unit with overlying sandstone (Lower Goyder Fm, 300m); upper sst/siltstone (Upper Goyder Fm, 300m) with unconformity between.||||||13-SEP-18
7646|Goyder Formation|65342|5|Briefly described|p4.|||Amadeus Basin.Max. thickness at least 145 m.||||Overlies Shannon Formation. Is overlain by Pacoota Sandstone.|Yellow-brown, partly micaceous kaolinitic sandstone.|
7646|Goyder Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Topmost unit in Pertaoorrta Group.||Overlies Shannon Formation. Is overlain by Pacoota Sandstone (Larapinta Group).||
7646|Goyder Formation|67126|5|Briefly described|p1, p3-9, p11-13, p20, p26, p33, p36-37|Middle Cambrian|Middle Cambrian|Amadeus Basin. Poor gas shale candidate: very low organic carbon content. Rock Eval analysis, Rock Eval Temperature Programme: Pyrolysis, Thermovaporisation, Pyrolysis Gas Chromatography results presented in detail.||||||
7646|Goyder Formation|67128|6|Mentioned|p30|||Northeastern Amadeus Basin.||||||
7646|Goyder Formation|67326|5|Briefly described|p2|Late Cambrian|Late Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Cleland, Petermann and Deception Sandstones, Hugh River Shale, Jay Creek Limestone and Shannon Formation. Is overlain by Pacoota Sandstone.||
7646|Goyder Formation|67565|4|Described|pp40-41, p47.|Late Cambrian|Late Cambrian|Peritidal sand and minor carbonate deposited during a marine transgression. Poorly exposed. Thickness decreases from 550 m near Stokes Pass, to 90 m in the west.||||Conformably overlies Petermann and Cleland Sandstones.|Dominantly a yellow-brown or buff, partly micaceous, fine to medium kaolinitic sandstone; thinly-bedded, cross-bedded and moderately well-sorted, with rippled surfaces; local thin stromatolitic limestone bed.|
7646|Goyder Formation|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
7646|Goyder Formation|68316|5|Briefly described|p778 Fig.1, p783 Fig.4, p784|Series 2|Series 2|Amadeus Basin.|c. 520 Ma (Zhao et al. 1992)|Of the Pertaoorta Group.||Underlain by the Arumbera Formation.||
7646|Goyder Formation|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Late Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
7646|Goyder Formation|69437|5|Briefly described|p22:10|Furongian|Series 3|Amadeus Basin.||||Overlies Cleland, Petermann Sandstones, Deception Formation. Is overlain by Pacoota Sandstone.||12-JUL-16
7646|Goyder Formation|69438|3|Fully described|p23:2-3,6-8,24-25,30-34,43,53,55-56,61|Late Cambrian|Late Cambrian|Defined by Pritchard and Quinlan (1962); redefined as a Member of the then Pertaoorrta Formation by Wells et al. (1965). Subsequently restored to Formation rank within the Pertaoorrta Group by Ranford et al. (1965). Up to 600m thick in Ooraminna Sub-basin, Amadeus Basin. A significant unconformity separates the lower and upper parts of the Formation. Grades laterally into Cleland Sandstone. Is overlain unconformably by Pacoota Sandstone. Various fossils listed. Sediment source was mainly from the Musgrave Province with lesser Arunta Region input. Hosts the Owen Springs uneconomic Cu-Pb-Zn occurrences. Drilled for oil, gas and shale oil in Johnstone West-1 and Surprise-1 wells, successfully. Has low shale gas potential.||Uppermost Pertaoorrta Group.||Conformably overlies Shannon Formation, Hugh River Shale, Jay Creek Limestone (also partial lateral equivalent), Cleland Sandstone and (also interfingers with) Petermann Sandstone.|A 300m interval of medium to thick interbeds of dolomitic ooid grainstone and cross-bedded sandstone, with  minor siltstone, calcareous mudstone, cryptalgalaminite, and intraclastic conglomerate, under 300m of fine to coarse sandstone and siltstone.|12-JUL-16
7646|Goyder Formation|69444|6|Mentioned|p29:2 Fig.29.3|||Amadeus Basin. Detrital zircon probability distribution diagram.||||||12-JUL-16
7646|Goyder Formation|69449|6|Mentioned|p34:2 Fig.34.2|Cambrian|Cambrian|Eastern Amadeus Basin.||||||12-JUL-16
7646|Goyder Formation|69573|6|Mentioned|p661|||Amadeus Basin.||||||
7646|Goyder Formation|70744|6|Mentioned|p944-945|Early Cambrian|Early Cambrian|Amadeus Basin. Detrital zircon age distribution graph.||||||
7646|Goyder Formation|70749|6|Mentioned|p54|||Amadeus Basin.||Pertaoorrta Group.||||
7646|Goyder Formation|70752|5|Briefly described|p126 Fig.1|Cambrian|Cambrian|||Pertaoorrta Group.|||Silty sandstone with minor siltstone; fossiliferous and stromatolitic dolostone with minor limestone.|
7646|Goyder Formation|71114|5|Briefly described|p171, p170 fig 1b, p172-180|Stage 10||Across entire Amadeus Basin. Unit includes a hiatus between carbonate-rich lower succession and sandstone-rich  upper succession with poor age control. Deposited between ~511 and 490 Ma. Marks rising sea level with flooding of nearshore sandstones and siltstones and subsequent deposition of shallow marine carbonates. 188m thick in Dingo 1 well. Age of the unit ranges from Guzhangian to Stage 10 based on trilobite biostratigraphy.||||Overlies Shannon Formation, Jay Creek Limestone and Petermann Sandstone.|Sandstone, siltstone, carbonates; alternating siltstones and dolostones indicate basin-wide transgression.|14-FEB-18
7646|Goyder Formation|71279|5|Briefly described|p355 Fig.2, p363, p365-366, p382 Tb.1|Late Cambrian|Late Cambrian|Amadeus Basin. Modelled magnetic properties.||Pertaoorrta Group.|||Limestone. See also p353.|27-OCT-17
7646|Goyder Formation|71800|5|Briefly described|p26-p27|Late Cambrian|Late Cambrian|Amadeus Basin.||||Overlies the Shannon Formation. Unconformably overlain by the Pacoota Sandstone.|Calcarenite.|
7646|Goyder Formation|71898|4|Described|iii, p1, p3, p17-p19|Late Cambrian|Late Cambrian|Amadeus Basin. This unit was defined by Pritchard and Quinlan (1962) before being redefined as a member of the then Pertaoorrta Formation by Wells et al (1965). Ranford et al (1965) subsequently restored the unit to formation status and included it in the Pertaoorrta Group. SHRIMP age is interpreted to be a maximum depositional age and is only slightly older than a terminal Cambrian (Payntonian; 491-488Ma) age derived from palynological evidence. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed. This unit has a maximum thickness of 600m in the northeast Amadeus Basin. This unit is subdivided into a lower and upper unit both deposited in shallow subtidal to intertidal environments. Dated sample is from within the unit, well below the contact with overlying Pacoota Sst and many hundreds of  m above Petermann Sst.|505 +/- 6 Ma (SHRIMP U-Pb)|Pertaoorrta Group|Includes the Goyder Formation, lower and Goyder Formation, upper.|Conformably (transitional) overlies the Petermann Sandstone. Unconformably overlain by the Pacoota Sandstone.|Fine- to medium-grained sandstone.|19-NOV-18
7646|Goyder Formation|72358|5|Briefly described|p116-121,123-125|Furongian|Furongian|Of Amadeus Basin. Laterally extensive across the Amadeus Basin, marking rising sea level and regional flooding. Inconsistencies regarding historical logging and stratigraphic position in legacy well interpretations e.g. lower contact at ~1170m in Alice 1, vs 761m in Wallaby 1, 7km E of Alice 1, but with similar GR log patterns. Equivalent to Georlina Limestone in the Georgina Basin.||||Overlain by Pacoota Sandstone. Overlies the Shannon Formation.|Shallow marine carbonates.|10-JAN-20
7646|Goyder Formation|72369|5|Briefly described|p26|||Of Amadeus Basin.||||Overlain unconformably by Pacoota Sandstone.||
7646|Goyder Formation|72489|5|Briefly described|p3-6, p7 Fig.6, p8, p9, p11,p12|Furongian|Guzhangian|Located in the Amadeus Basin. Age based on trilobite stratigraphy. Formed during periods of intense continental chemical weathering.||||Overlain by Julie Formation. [Said to be overlain by Wonoka Fm but this unit in Adelaide Rift Complex]|Carbonate.|
7646|Goyder Formation|72516|6|Mentioned|p93|Cambrian|Cambrian|Amadeus Basin.||||Lower part equivalent to the Arrinthrunga Formation.||08-JUN-21
7646|Goyder Formation|73085|6|Mentioned|p1, p4|late Cambrian|late Cambrian|||Pertaoorrta Group [and equivalents?]||Overlain by Pacoota Sandstone (Larapinta Group).||
7696|Grant Group|7142|6|Mentioned|p351. |||Canning Basin.||||||
7696|Grant Group|7433|4|Described|p25 Fig.2, p32 Fig.8, p33, pp36-37.|Permian|Early Permian|Canning Basin. Fine to coarse clastics, glaciomarine to fluvioglacial. Clasts derived from Precambrian cratonic sequences. Excellent aquifer with basinwide extent; confined by Noonkanbah Formation. Possible coal prospectivity.|||Has three sub-divisions: Betty, Winifred and Carolyn Formations.|Underlies Poole Sandstone; unconformably in the Fitzroy Sub-basin.|Diamictites and laminated clastic sediments with dropstones; quartz sandstone. Diamictites: small pebble- to large boulder-sized rounded clasts, often striated and facetted; matrix often feldspathic.|
7696|Grant Group|22718|5|Briefly described|P5, Table1 P7|Sakmarian|Late Carboniferous|||||||
7696|Grant Group|22738|4|Described|6,10,12,16-18, map|Early Permian|Early Permian|Max thickness 1000 m. Overlying units Wallal Sandstone, Poole Sandstone, underlying units Carribuddy Formation, Nita Formation, Goldwyer Formation, Willara Formation, Nambeet Formation.||||||17-JUN-09
7696|Grant Group|22741|5|Briefly described|P24, P25, Table3 P14||Permian|Formerly Grant Formation.||||||10-NOV-08
7696|Grant Group|22753|4|Described|p 533, Fig.3 p585|Permian|Carboniferous|See also p535.||||||11-APR-08
7696|Grant Group|22765|5|Briefly described|P9, Table1|Sakmarian|Late Carboniferous|Maximum thickness is 398m, Overlying unit is Poole Sandstone||||||
7696|Grant Group|22767|5|Briefly described|Table3 P16, P21|Early Permian|Late Carboniferous|||||||
7696|Grant Group|22776|6|Mentioned|Table.3|Early Permian|Early Permian|||||||
7696|Grant Group|22801|5|Briefly described|P11, Table1 P9||Sakmarian|||||||
7696|Grant Group|22814|5|Briefly described|fig2|Early Permian|Carboniferous|||||||
7696|Grant Group|23212|4|Described|Table.1 p7||Early Permian|||||||
7696|Grant Group|23415|6|Mentioned|Map Legend (Simplified geol.)|||Geological province: Canning Basin.||||||07-JAN-08
7696|Grant Group|23523|4|Described|p994|Permian|Permian|See also p997. Geological Province: Canning Basin.||||||
7696|Grant Group|23558|5|Briefly described|p37|||||||||
7696|Grant Group|23575|5|Briefly described|Map Legend|Permian|Permian|||||||
7696|Grant Group|23722|4|Described|p35|Early Permian|Late Carboniferous|Geological Province: Canning Basin.||||||11-APR-08
7696|Grant Group|23726|6|Mentioned|p43|||Geological Province: Canning Basin.||||||
7696|Grant Group|23757|5|Briefly described|p5,  p16|Early Permian|Early Permian|Formerly Grant Formation. Geological Province: Canning Basin.||||||07-JAN-08
7696|Grant Group|23765|5|Briefly described|Map Legend|Permian|Carboniferous|||||||23-DEC-09
7696|Grant Group|23766|5|Briefly described|p14 Tb. 2|Permian|Permian|||||||
7696|Grant Group|23903|5|Briefly described|p1597 Fig.2|Permian|Permian|Geological Province: Canning Basin||||||
7696|Grant Group|24246|5|Briefly described|p15|Permian|Carboniferous|Geological Province: Canning Basin.||||||
7696|Grant Group|24390|5|Briefly described|p6 Fig. 4|Permian|Carboniferous|Geological Province: Canning Basin.||||||
7696|Grant Group|24449|5|Briefly described|p740, p741 Fig. 2|Sakmarian|Stephanian|Age: <300m.y.  Geological Province: Canning Basin.||||||
7696|Grant Group|24466|5|Briefly described|p365|Permian|Permian|||||||
7696|Grant Group|35127|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35201|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35202|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35207|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35222|4|Described|Table.2|||||||||
7696|Grant Group|35223|4|Described|Table.2|||||||||
7696|Grant Group|35225|4|Described|Table 1|||||||||
7696|Grant Group|35226|4|Described|Table 1|||||||||
7696|Grant Group|35250|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35251|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35252|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|35387|6|Mentioned|Map legend|Permian|Permian|||||||
7696|Grant Group|35497|4|Described|Table 1|||Also on P10||||||
7696|Grant Group|35902|4|Described|Table 1|||||||||
7696|Grant Group|35903|4|Described|Table 1|||||||||
7696|Grant Group|36224|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Includes: Carolyn, Winifred and Betty Formations.  Late Carboniferous to Early Permian.||||||01-FEB-05
7696|Grant Group|36225|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
7696|Grant Group|36257|6|Mentioned|Table 2.1|||||||||
7696|Grant Group|36438|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|36632|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|36634|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
7696|Grant Group|37212|6|Mentioned|p17|||||||||
7696|Grant Group|37368|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|37369|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|37370|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|37914|3|Fully described|p449|||||||||08-FEB-10
7696|Grant Group|38732|6|Mentioned|p33|||||||||
7696|Grant Group|38878|6|Mentioned|Map legend|Sakmarian|Stephanian|Stephanian - Sakmarian||||||
7696|Grant Group|38886|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
7696|Grant Group|39757|6|Mentioned|p1606|||||||||
7696|Grant Group|39854|6|Mentioned|p21|||||||||
7696|Grant Group|39857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|40045|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|40078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
7696|Grant Group|40838|6|Mentioned|p279|||||||||
7696|Grant Group|40901|6|Mentioned|p62|||||||||
7696|Grant Group|40992|6|Mentioned|p5|||||||||
7696|Grant Group|41023|6|Mentioned|p292|||||||||
7696|Grant Group|41125|5|Briefly described|p41|||||||||
7696|Grant Group|41158|6|Mentioned|p73|||||||||
7696|Grant Group|41169|6|Mentioned|p148|||||||||
7696|Grant Group|41215|6|Mentioned|p281|||||||||
7696|Grant Group|41283|6|Mentioned|p80|||||||||
7696|Grant Group|41315|4|Described|p135|||||||||
7696|Grant Group|41436|6|Mentioned|p39|||||||||
7696|Grant Group|41449|5|Briefly described|p256|||||||||
7696|Grant Group|41688|5|Briefly described|Table 4|||||||||
7696|Grant Group|41689|6|Mentioned|Table 1|||||||||
7696|Grant Group|41828|6|Mentioned|p497|||||||||
7696|Grant Group|41839|4|Described|p25|||Formerly "Grant Range Beds", "Grant Formation".||||||11-APR-08
7696|Grant Group|42080|5|Briefly described|p281|||See also Fig.2||||||
7696|Grant Group|42191|6|Mentioned|p437|||||||||
7696|Grant Group|42309|6|Mentioned|p246|||||||||
7696|Grant Group|42338|5|Briefly described|Table 1 P145|||||||||
7696|Grant Group|42347|4|Described|p1020 Fig.2|||||||||
7696|Grant Group|42392|6|Mentioned|p115|||||||||
7696|Grant Group|42547|4|Described|p96|||||||||
7696|Grant Group|42571|5|Briefly described|p20, Table1 p9|||||||||
7696|Grant Group|42572|5|Briefly described|Map Legend|Permian|Carboniferous|||||||23-DEC-09
7696|Grant Group|42613|1|Redefined|p2|||Formerly Grant Formation. See subdivisions Carolyn, Winifred & Betty Formations.||||||10-NOV-08
7696|Grant Group|42710|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
7696|Grant Group|42711|6|Mentioned|p19|||Geological province: Canning Basin. Equivalent to Shotts Formation in the Collie Basin.||||||11-AUG-08
7696|Grant Group|42792|5|Briefly described|Table 1 P225|||||||||
7696|Grant Group|42811|4|Described|p44|||||||||
7696|Grant Group|42814|5|Briefly described|p23|||||||||
7696|Grant Group|42815|5|Briefly described|map|Early Permian|Late Carboniferous|||||||
7696|Grant Group|42880|5|Briefly described|p1020|||||||||
7696|Grant Group|43015|5|Briefly described|Table 1,p319|||||||||
7696|Grant Group|43018|5|Briefly described|Table 1,p386|||||||||
7696|Grant Group|43050|5|Briefly described|p8|||||||||
7696|Grant Group|43142|5|Briefly described|p178|||||||||
7696|Grant Group|43281|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||||||
7696|Grant Group|43442|6|Mentioned|p27|||||||||
7696|Grant Group|43563|6|Mentioned|Fig.2,p5|Early Permian|Early Carboniferous|||||||
7696|Grant Group|43666|6|Mentioned|p7||Permian|||||||
7696|Grant Group|43812|6|Mentioned|p157|||||||||
7696|Grant Group|43816|5|Briefly described|p87|Permian|Carboniferous|||||||
7696|Grant Group|43818|6|Mentioned|Fig.2.p39|Early Permian|Late Carboniferous|||||||
7696|Grant Group|43823|5|Briefly described|p753|Early Permian|Late Carboniferous|Herein subdivided into Lower Grant Group and Upper Grant Group.||||||
7696|Grant Group|44143|4|Described|p436, p445, p447 Fig.4-103|Permian|Carboniferous|Includes Betty, Winifred and Carolyn Formations. Sandstone, conglomerate, siltstone, mudstone.||||||23-NOV-17
7696|Grant Group|44231|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Massive, medium- to coarse-grained silty sandstone and siltstone, and boulder conglomerate; fluvial, lacustrine, glacially influenced  in part. Geological Province: Canning Basin.||||||18-MAY-05
7696|Grant Group|44357|4|Described|p12,Tb.1 p9||Early Permian|Subsurface only. Inferred from drilling in surrounding sheet areas.||||||
7696|Grant Group|44443|5|Briefly described|map legend|Early Permian|Early Permian|||||||
7696|Grant Group|45149|6|Mentioned|Table 1|||Page 15.||||||
7696|Grant Group|45158|3|Fully described|p22|||See also p11.||||||10-NOV-08
7696|Grant Group|45168|6|Mentioned|p6|||||||||
7696|Grant Group|46319|4|Described|p17|Early Permian|Early Permian|||||||
7696|Grant Group|49644|5|Briefly described|Table|||||||||
7696|Grant Group|50085|5|Briefly described|p6 Fig. 4|Permian|Carboniferous|Geological Province: Canning Basin.||||||
7696|Grant Group|50544|6|Mentioned|p16 Tb. 1|Early Permian|Early Permian|No surface exposure on the YARRIE sheet.  Age: c.288-280Ma.  Overlain by the Liveringa Group and Wallal Sandstone.  See also p62.||||||07-OCT-04
7696|Grant Group|50555|5|Briefly described|Map legend|Permian|Permian|Sandstone, siltstone, claystone.  Geological Province: Canning Basin.||||||
7696|Grant Group|60295|5|Briefly described|p136|||Geological Province: Canning Basin.||||||
7696|Grant Group|60386|5|Briefly described|p291, 297, p309|Sakmarian|Asselian|Canning Basin. Post-Visean, post Alice Springs Orogeny glacial deposits. Deltaic - nearshore - shelf. ||||||
7696|Grant Group|61021|5|Briefly described|p36 Fig. 2|Sakmarian|Asselian|Includes the Winifred Shales. Geological Province: Canning Basin. See also p37.||||||17-DEC-07
7696|Grant Group|61023|5|Briefly described|p10 Fig. 6|Permian|Carboniferous|Geological Province: Canning Basin.||||||11-APR-08
7696|Grant Group|61139|5|Briefly described|p42 Fig. 4|Early Permian|Late Carboniferous|Geological Province: Canning Basin.||||||09-JUN-05
7696|Grant Group|61551|6|Mentioned|p351 Fig.2, p359, p361. |Sakmarian|Moscovian|Oil sourced from the Laurel Formation is produced from this Group at the Boundary, Sundown and West Terrace fields.||||Is overlain by Poole Sandstone.||
7696|Grant Group|64186|6|Mentioned|p177|||Sediments.||||||
7696|Grant Group|64502|5|Briefly described|p764, p768, Fig.5|Sakmarian|Asselian|||||||27-JAN-10
7696|Grant Group|64580|4|Described|map legend|Early Permian|Pennsylvanian|Sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene; includes HOYA, CALYTRIX, CLIANTHUS, BETTY, WINIFRED, and CAROLINE[Carolyn] FORMATIONS.||||||09-FEB-18
7696|Grant Group|64630|5|Briefly described|p31 Fig.2, p33, 35, 37|Sakmarian|Bashkirian|Province: Northern and Central Canning Basin. Underlies the Poole Sandstone, includes: Carolyn, Clianthus, Calytrix and Hoya formations; also includes Winifred Formation, Reeves Formation. Palynology age: S. ybertii to P. confluens.||||||24-NOV-09
7696|Grant Group|64643|5|Briefly described|p3 Fig. 2, p5, fig.4, p20|Cisuralian|Cisuralian|Lower Permian(?Asselian - early Sakmarian). Disconformably overlies Reeves Formation in Fitzroy Trough.||||||17-NOV-08
7696|Grant Group|64970|6|Mentioned|p720|||Equated to the Paterson Formation in the Officer Basin. Geological Province: Canning Basin.||||||27-MAY-09
7696|Grant Group|64971|1|Redefined|p683-686, including p685 Fig. 2|Early Permian|Visean|Formation of Guppy et al. (1952), was previously Grant Range Beds. Raised to Group status (Crowe and Turner 1976); Group redefined here: retains Hoya, Calytrix and Clianthus Formations (Redfern and Millward 1994). Under Poole Sandstone, erosional contact.||||||09-FEB-10
7696|Grant Group|64974|5|Briefly described|p148 Fig. 6|Early Permian|Late Carboniferous|Includes; Betty, Winifred and Carolyn Formation. Geological Province: Canning Basin.||||||
7696|Grant Group|64981|5|Briefly described|p669 Fig.3.|Sakmarian|Late Carboniferous|Produces oil in the Boundary oil field; correlated with Betty Formation. Sourced probably from Laurel Formation.|||Includes Betty, Winifred and Carolyn Formations.|Unconformably overlies Anderson Formation. Is overlain by Poole Sandstone.||
7696|Grant Group|64982|5|Briefly described|p699 Fig.4.|Tatarian|Late Carboniferous|Up to 300 m of fluvio-glacial to marine deposits. Contains marine macrofossils, crinoids, bryozoans and palynomorphs.|||Includes Betty, Winifred and Carolyn Formations.|Unconformably overlies Mellinjerie Limestone.||
7696|Grant Group|65102|6|Mentioned|p375|Permian|Permian|Canning Basin. Deposited in open marine environment. Correlated with glacial to subglacial lacustrine to fluvial Paterson Formation of Officer Basin.||||||
7696|Grant Group|65301|5|Briefly described|p3, p5 Fig. 4|Early Permian||Overlain by Poole Sandstone, Noonkanbah Formation and units of the Liveringa Group. Geological province: Canning Basin. A partly glaciogene group; commonly contains porous sandstones with good reservoir properties. See also p8 Fig. 5.||||||
7696|Grant Group|65449|5|Briefly described|p5-6, p10-11, p17, p37, p47-48, p51-52|Cisuralian|Cisuralian|Widespread, non-marine to marine siliciclastics with glacially-influenced deposits near the base. Base of Megasequence III of Warris (1993). Oil from this unit could be explained as a mixture of oils similar to those recovered from Willara and Nita Formations, with an extra source.||||Unconformably overlies Reeves Formation and Carribuddy Group. Is overlain unconformably by Poole Sandstone.||
7696|Grant Group|65486|5|Briefly described|p4, p9 Fig. 7, p18, p28-30|Sakmarian|Asselian|Canning Basin. Contains at its base Carolyn Formation. Overlies Fairfield Group and Prices Creek Group with a planar glacial unconformity; deposited on a near-horizontal and karstified surface. Glacial grooves in sandstone of this unit in the Grant Range indicate ice sheet movement to N or NNW.||||||
7696|Grant Group|65826|6|Mentioned|p16.|Permian|Carboniferous|Canning Basin. Deposited in a graben-like structure called the Waukarlycarly Embayment.||||||
7696|Grant Group|66127|3|Fully described|p61, p212, p215, p234-242, Pl. 2,3,4,5,7|Sakmarian|Asselian|Sediments deposited at end of Permo-Carboniferous glaciation; N- to NW-directed glacial grooves are locally preserved. Locally overlies Proterozoic basement.|||Includes Carolyn Formation at the base.|Unconformably overlies Bugle Gap Limestone, Prices Creek Group, Fairfield Group. Is overlain by Poole Sandstone.|Crudely bedded marine sandstone and siltstone; in part glacigene; includes boulder-bearing tillite.|
7696|Grant Group|66949|4|Described|p1, p4 Fig.2, p6-23, p28, p31-33|Sakmarian|Asselian|See also p46-54 Appx.2, p57-58 Appx.3, p60-65 Appx.4, p66-94 Appx.5; p119-120 Appx.7; Plates 2-7, 9-10,12. Crowe and Towner, (1976). Originally Grant Range Beds (Woolnough, 1933); later Grant Formation (Guppy et al., 1952). Named after Grant Range. Basal glacial succession in Canning Basin. Composite section detailed. Up to ?1000m thick; non-marine and marine glacial deposits. Biostratigraphic zonation. Difficulties in sub-dividing this Group are discussed. Reservoir and sealing properties discussed. Good to excellent hydrocarbon source potential. Available core and Formation picks detailed. Several dolerite intervals in lower part, aged 291 +/- 2 Ma (K-Ar) and 255 +/- 13 Ma (fission track). TOC and Rock-Eval data.|||Includes Carolyn, Winifred, Betty, Clianthus, Calytrix and Hoya Formations.|Overlies Reeves Formation conformably to disconformably. Is overlain disconformably by Poole Sandstone.|Dominantly sandstone; also diamictite, conglomerate and mudstone.|
7696|Grant Group|67202|5|Briefly described|p34, p37 Fig.2.6, p43, p44 Fig.2.10, p67|Permian|Permian|See also p126, p128, p135. Fluvio-glacial and marine sediments. Conductivity images.|||Paterson Formation.||Fine to coarse sandstone; shale, siltstone, conglomerate.|
7696|Grant Group|67354|6|Mentioned|p107.|||Lennard Shelf, Canning Basin. Possibly contains tunnel valleys.||||||
7696|Grant Group|67856|6|Mentioned|p348|||Of Canning Basin.||||In part correlated with Buck Formation and Ligertwood beds.||
7696|Grant Group|67888|6|Mentioned|p42|Triassic|Carboniferous|Good oil reservoir potential identified.||||||
7696|Grant Group|68007|4|Described|p1-2, p4, p6-7, p9-10, p12, p14-15|Early Permian|Early Permian|See also Plates 1, 2. Canning Basin. 711m thick in Patience 2 well. Good to excellent reservoir potential. Intra-Group shales are potential seals over Permian reservoirs. Characterised by high frequency facies changes and channelling. Composite well log. Early Permian: ?Asselian to early Sakmarian, based on palynomorphs from the P. confluens Zone.|||Includes Betty, Winifred and Carolyn Formations; Hoya, Calytrix and Clianthus Formations.|Overlies Reeves Formation probably conformably. Unconformably overlies Clapp Ridge Formation. Is overlain by Poole Sandstone.|Predominantly siliciclastic succession of fluvial to shallow-marine origin with glacial influence.|20-FEB-20
7696|Grant Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Sakmarian|Pennsylvanian|Canning Basin. See also 500k_geologyp08_lut.csv.|||Includes Hoya, Calytrix, Betty, Winifred and Caroline (misspelling of Carolyn) Formations.||Undivided; sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene.|26-NOV-15
7696|Grant Group|68902|5|Briefly described|p1-2, p8-10, p22-26|Permian|Permian|Defined (Veevers and Wells, 1961) in northern Canning Basin. Overlies a thick succession in the Wallal Embayment, comparable to one in the Waukarlycarly Embayment. 300-800m thick. ?Asselian to Early Sakmarian.|||Includes Paterson Formation|Overlies Paterson and Nambeet Formations. Unconformably (locally conformably) overlies Reeves Formation. Is overlain unconformably by Poole Sandstone.|Diamictite, sandstone and siltstone of fluvial to marine glacigene origin.|18-JAN-17
7696|Grant Group|69029|5|Briefly described|p319,321|Sakmarian|Asselian|Of Canning Basin. Proven reservoir rock to the Boundary, Sundown, and West Terrace oilfields on the Lennard Shelf, sealed by shale unit in the Poole Sandstone and Blina Shale.||||Overlain by Poole Sandstone. Underlain by Reeves Formation or Fairfield Group or Tandalgoo Sandstone/Worral Formation.||
7696|Grant Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Sakmarian|Pennsylvanian|Canning Basin|||||Sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene.|31-JUL-15
7696|Grant Group|69165|4|Described|500k_geologyp08_lut.csv|Cisuralian|Pennsylvanian||||Includes Hoya Formation, Calytrix Formation, Clianthus Formation, Betty Formation,  Winifred Formation, Caroline Formation||Undivided; sandstone, siltstone, diamictite, conglomerate and shale; largely glacigene;|
7696|Grant Group|69182|5|Briefly described|Ch4 p3, Ch4 p9, Ch4 p15-p16|Cisuralian|Pennsylvanian|Canning Basin. Deposited during a period of regional glaciation. Contains local to regional seal units. See also Ch4 p20-p25, Ch4 p30-p35, Ch4 p38-p39, Ch4 p43-p44, Ch4 p45, Ch4 p48, Ch4 p50-p58, Ch4 p62-p65, Ch4 p67, Ch4 p74-p77, Ch4 p83-p84, Ch4 p87-p91, Ch4 p96.  |||Includes the Winifred Formation.|Overlies the Reeves, Goldwyer and Nambeet Formations. Overlain by the Poole Sandstone.|Fluvial to shallow-marine sandstones and claystones.|19-MAR-20
7696|Grant Group|69297|6|Mentioned|p337, p350, p351, p352, p355|Sakmarian|Sakmarian|Broome Platform of the Canning Basin. |||Includes the Reeves Formation, Hoya Formation, Calytrix Formation, Clianthus Formation, Poole Sandstone and the Noonkanbah Formation.|Unconformably overlies the Fairfield Group.||
7696|Grant Group|69312|6|Mentioned|p3, p13 fig 13-14, p14 fig 15|Sakmarian|Asselian|Canning Basin. See also  p15, p19, p23 fig 26-27, p24 fig 28-29, p25 fig 30-31, p26 fig 32-33, p27, p27 fig 34, p28 fig 35-36, p29 fig 37. ||||Overlies the Reeves Formation. Overlain by the Poole Sandstone.|Sandstone.|
7696|Grant Group|69547|4|Described|p182,190|Sakmarian|Asselian|Canning Basin. Thick sandstone-dominated succession that is interpreted as either glacially influenced (Redfern and Millward, 1994) and/or resulting from phases of local tectonic subsidence with some reworking of glacial sediment (Eyles and Eyles, 2000).||||Overlain by Nura Nura Member/Poole Sandstone.|Grey shale.|
7696|Grant Group|69587|4|Described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv. |323.2-290.1 Ma (inferred)||||Sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene|
7696|Grant Group|69634|4|Described|GEOL_LUT_CSV files|Early Permian|Pennsylvanian|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|323.1-290.1 Ma (Inferred)||Includes Hoya, Calytrix, Betty, Winifred, Clianthus and Caroline formations.||Undivided; sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene|
7696|Grant Group|69660|5|Briefly described|Map legend|Permian|Carboniferous|Canning Basin.|||||Sandstone, siltstone, diamictic, conglomerate and shale; largely glacigene.|
7696|Grant Group|69693|5|Briefly described|p1-5, 8-10|Permian|Carboniferous|Canning Basin. Serpukhovian to Sakmarian. Contains a series of large NW-SE anastomosing channels on the Lennard Shelf, attributed to the last phase of Permo-Carboniferous glaciation.|||Carolyn, Betty, Winifred, Hoya, Calytrix, Cliantus Formations.|Unconformably overlies Anderson Formation. Is overlain unconformably by Poole Sandstone.|Glacial deposits. Includes sands and muds.|
7696|Grant Group|69883|6|Mentioned|p6, p34, |Permian|Permian|See also plate 1, plate 3.||||||
7696|Grant Group|70065|5|Briefly described|Rowley: Fig.2;p2. Regional: Fig.4;p3,p6|Sakmarian|Sakmarian|Roebuck Basin and offshore Canning Basin. A thick succession of glacial deposits. Permian sandstones form reservoirs, but the marine shales, while locally organic-rich, generally have poor generative potential. Hydrocarbon accumulations within the Group are believed to be sourced from the underlying Laurel Formation.||||Overlies Fairfield Group. Is overlain by Poole Sandstone.||
7696|Grant Group|70129|5|Briefly described|Map legend|Permian|Carboniferous|Canning Basin.|||||Sandstone, siltstone, diamictite, conglomerate and shale; largely glacigene.|
7696|Grant Group|70154|5|Briefly described|500k_interpgeop14_lut.csv|Sakmarian|Pennsylvanian|See also 250k_geologyp_lut.csv, 250k_geologyp_lut.csv.|290-323 Ma||||Sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene|
7696|Grant Group|70272|5|Briefly described|p878|Early Permian|Late Carboniferous|Lennard shelf, Canning Basin.||||Unconformably overlies Fairfield Group.|Sandstones.|
7696|Grant Group|70288|6|Mentioned|p414-415, 417-419|Pemian|Permian|NE margin of the Canning Basin. Intruded by diamondiferous lamproite pipes. Photographs.|||||Glaciogenic sandstones.|
7696|Grant Group|70492|6|Mentioned|p166, 168, 176-179|Permian|Permian|Canning Basin.||||Overlies Reeves Formation and, unconformably, Fairfield Group.||
7696|Grant Group|70774|5|Briefly described|p1, p4-p5, p7-10, p25-28|Early Permian|Late Carboniferous|Canning Basin. This group has potential as a petroleum reservoir. Stratigraphic columns are provided and lithology discussed in detail in appendix 2. See also p31-p32, p37-p38, p41, p49, p51-p54, p64, p66, p71, p93-p100, Plate 6.  Along with Poole Sandstone and Noonkanbah Formation, part of late Carboniferous - Permian Megasequence  deposited c. 330 to 243 Ma (Kennard et al. 1994).|||Includes the Hoya Formation, Clianthus Formation and the Calytrix Formation.|Overlies the Reeves Formation. Unconformably overlain by the Nura Nura Member (Poole Sandstone) and the Noonkanbah Formation.||10-FEB-20
7696|Grant Group|70812|5|Briefly described|p43|Permian|Permian|Overlies Devonian carbonate rocks.|||||Siliciclastic sedimentary rocks.|
7696|Grant Group|70826|6|Mentioned|p6 tbl 3|Early Permian|Late Carboniferous|northern Canning Basin.||||||
7696|Grant Group|70851|6|Mentioned|p19|||||||||
7696|Grant Group|70878|5|Briefly described|p722 Fig.17|Permian|Permian|Fitzroy Trough, NW Canning Basin.||||||
7696|Grant Group|71146|5|Briefly described|p6, p12 fig 8, p13, |Sakmarian|Late Carboniferous|Canning Basin, Lennard Shelf. See also p37,  p43 fig 33, p44.|ca 299 Ma|||Unconformably overlies the Reeves Formation. Disconformably overlain by the Poole Sandstone.|Sandstone.|
7696|Grant Group|71171|5|Briefly described|p7-p8|Permian|Permian|Replaced the Grant Formation of Yeates et al, 1975 and Yeates and Muhling, 1977.||||Unconformably overlies the Carranya Formation.|Thick, poorly sorted, imbricated, boulder conglomerate.|
7696|Grant Group|71267|4|Described|GEOL_LUT_CSV files|Sakmarian|Pennsylvanian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 1m_interpgeop_lut.csv.|323.2-290.1 Ma (inferred)||Includes Carolyn Formation.||Shallow marine to fluvial, and possibly partly glacial, cross-bedded fine to very coarse quartz sandstone, laminated micaceous sandstone, siltstone, mudstone, and minor conglomerate, fossiliferous; wood fragments and bioturbated in places.|
7696|Grant Group|71870|5|Briefly described|p3, p5|Sakmarian|Asselian|Canning Basin.||||Unconformably overlies the Reeves Formation and the Nambeet Formation. Overlain by the Poole Sandstone.||
7696|Grant Group|71892|5|Briefly described|p8, p10-p11, p16, p19-p20, p33|Permian|Permian|Intruded by Ellendale diamondiferous pipe 4 (E4).|||Includes the Poole Sandstone.||Fine- to medium-grained quartz and feldspathic quartz sandstone with less common horizons of fine-grained clayey sandstone or siltstone and coarse pebbly clayey quartz sandstone. Conglomerate.|
7696|Grant Group|71894|5|Briefly described|p3-p4, p12, p20, p27, p31|Cisuralian|Pennsylvanian|Canning Basin. Laterally extensive across the basin.||||Unconformably overlies the Reeves Formation. Disconformably overlain by the Poole Sandstone. Equivalent to the Paterson Formation.|Sandstone and diamictite.|
7696|Grant Group|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Pennsylvanian|Glacigene rocks, Canning Basin. Age inferred.|||||Sandstone, siltstone, diamictite, conglomerate, and shale; largely glacigene.|
7696|Grant Group|72496|4|Described|p217-218, 220-231|Sakmarian|Asselian|Canning Basin. Diamictites, varved mudrocks and a glacial unconformity at the base of this group suggest a glacial depositional environment. A widespread middle shale unit encountered in most wells varies from between 27 to 81m in thickness. Thickness variation is complex in the Barbwire Terrace.|||Includes the Betty Formation, Winifred Formation, Carolyn Formation, Hoya Formation, Calytrix Formation and the Clianthus Formation.|Unconformably overlies the Reeves Formation and the Fairfield Group.||19-MAR-20
7696|Grant Group|72497|5|Briefly described|p4, p6 Fig.4, p12, p15, p16 Fig.9-10.|Sakmarian|Serpukhovian|After Redfern and Millward, 1994. Informally subdivided into Grant Group, lower and Grant Group, upper.  Deposited under fluvioglacial, shallow-marine, marginal-marine, and deltaic conditions. Reservoir qualities discussed. See also p19.|||Includes Carolyn Formation, Winifred Formation and Betty Formation, Hoya, Calytrix and Clianthus Formations.|Unconformably underlies Poole Sandstone. Unconformably overlies Anderson Formation.|Coarse grained sandstones with finer, thinner layers in lower parts. Includes some glaciogenic sediments such as dropstones and loosely consolidated sediment.|
7696|Grant Group|72499|4|Described|p1-2, p5, p6, p7, p8, p10-11.|Cisuralian|Pennsylvanian|Variable thickness from 1100m in Fitzroy Trough to 300-400m on Broome Platform. Proposed as a potential reservoir for CO2 geosequestration, due in part to the occurence of intra-formational mudstones. Located in the Willara Sub-basin, Broome Platform and the Fitzoy Trough.  See also p14-32, p35, p38, p43, p46-47, p49, p53, p54, p57-61, p66-68, p71, p75-76, p81-86, p88-96, p98-101.|||Includes Carolyn Formation, Winifred Formation, Betty Formation|Unconformably overlies Reeves Formation and underlies Poole Sandstone. Shown as unconformably overlying Fairfield Group. Laterally equivalent to Peterson Formation.|Dominated by coarse siliciclastic facies and intercalated muddy facies. Includes glacigenic sediments, diamictites, turbidites and mudstone, with fluvial-shallow marine sandstone, cross-bedded sandstone.|
7696|Grant Group|72502|6|Mentioned|p3|||||||||
7696|Grant Group|72504|5|Briefly described|Figure 1-3|Early Permian|Early Permian|Canning Basin. Extends across the entire Canning Basin with a maximum thickness of 2000m at Grant Range (1600m in Grant Range 1 and 400m in surrounding outcrop). Biostratigraphy is discussed. Displays abundant glacial features.||||||18-MAR-20
7696|Grant Group|72505|5|Briefly described|p890, 893|Asselian|Carboniferous|Canning Basin. Correlates with the Microbaluspora tentula and P.confluens zones.||||Unconformably overlain by the Poole Sandstone.||
7696|Grant Group|73117|3|Fully described|[See comments].|Asselian|Kasimovian|Widespread across the Canning Basin. Mostly fluvial strata; includes glacial characteristics such as striations, lonestones, diamictites, and U-shaped paleovalleys that appear to lie at different levels across the basin. Equivalent to glacial strata in other parts of Gondwana (supported by palynomorph data). Oldest part of the unit represents deglacial facies. Other suggested settings for parts of the group include a low-sinuosity fluvial systems (V-shaped paleovalleys), dendritic channels, deltas and possible marine influence, which may be related to the position of described sections relative to the axis of the Fitzroy Trough. No lithostratigraphic regional marker horizons. Maximum thickness of ~2 km in the central Fitzroy Trough. Thickness variations on the Broome Platform related to underlying Ordovician salt. Onlaps onto older units, especially along the margins of the basin. Authors suggest the use of this name for the main part of the Canning Basin whereas scattered outcrops of the [Grant Group equivalent] that overlie Precambrian basement elsewhere should be called Paterson Formation. Previously included strata now defined as the Reeves Formation and distinguishing between the two is highly reliant on palynozonation. Includes the spore-pollen zones Vallatisporites arcuatus, Microbaculispora tentula and Pseudoreticulatispora confluens; the first of which is established herein. [Article includes detailed palynomorph biostratigraphy]. Dark spore-pollen indicate the base lies below the oil window. Thermal maturity data indicate deeper parts may be/have been within the oil window. Other data indicates low-generating potential but may be suitable for reservoir-seal couplets including [sandstones] with up to 35% porosity and mudstones that can form effective top seals. p: 1-3, 5, 11-19, 21-39, 52, 54, 56, 61, 63, 65, 70, 72, 109-111, 113-132, 135-142.||||Unconformably underlain by Reeves, Laurel, Worral[?], Luluigui, and Clanmeyer formations, and Carribuddy Group. Disconformably overlain by Poole Sandstone including the Nura Nura Member.|Siliciclastic succession, dominantly glacio-fluvial origin composed of sandstone, mudstone, conglomerate and diamictite.|
7696|Grant Group|73184|4|Described|p183-184, p186-189, p192, p194-202|Sakmarian|late Pennsylvanian|Canning Basin, outcrops along the north, south and east basin margins. Post-rift succession, unconformably overlies Ordovician to Carboniferous strata. Age largely constrained by palynology, foraminifera-brachiopod-gastropod assemblages and palynomorphs from the latest Pennsylvanian (?Gzhelian in text) to Asselian or early Sakmarian. Lower absolute age limit of ca 296 Ma from eastern Australia palynozones (Black et al., 2003). Multiple erosion surfaces, predominantly but not exclusively in lower Grant group intervals. Evidence of glacial origin includes striated and faceted clasts within glaciogenic facies, intraformational iceberg striae, cold-water marine fauna, ice-rafted debris. Deposited in glaciated shallow marine and proglacial fluvial-deltaic environments with turbidite/glacial density flow successions and shoreline regression in the northern Canning Basin. Broadly equivalent to the P1 glacial phase in eastern Australia (Fielding et al., 2008). Detrital zircons sourced from the Arunta Inlier and Musgrave Province with lesser components from north and south of the Canning Basin.|297 +/- 7 Ma, 303.8 +/- 2.8 Ma, U-Pb zircon|||Overlies the Reeves Formation, underlies the Poole Sandstone.|Basal lithologies of glacial diamictite, conglomerate, coarse-grained sandstones. Upper facies associations include fossiliferous glaciomarine mudstones followed by fluvial-dominated delta systems with stacked cross-bedded channel sandstones.|
7696|Grant Group|73344|6|Mentioned|p2-3, p31, p55|Permian|Carboniferous|Canning Basin. Recovered from three cored intervals in the Samphire Marsh 1 well. Microbaculispora tentula palynozone [tentatively] identified in Olympic 1 well between 760-860 m.||||Unconformably underlain by Samphire Marsh Member (Nambeet Formation).||
7696|Grant Group|73345|5|Briefly described|p224, p226-227, p229-231|Sakmarian|Kasimovian|Canning Basin, widespread. Could constitute a seal for CO2 storage in the underlying Barnicarndy Formation in the Barnicarndy Graben. Broadly separated into lower and upper subdivisions. Represents a cyclical glacial depositional environment. Work on these strata from the Barnicarndy 1 well includes palynology, which indicated typical biostratigraphic units for the group.||||Underlain by Barnicarndy Formation (unconformably) and Reeves Formation. Overlain by Poole Sandstone. Equivalent to Paterson Formation.|Includes muddy diamictites, poorly sorted sandstones with soft-sediment deformation and rare pebble to cobble conglomerate.|
7696|Grant Group|73346|4|Described|p1-3, p5-7, p10, p16, p27-30, App.1|Asselian|Kasimovian|Canning Basin, widespread. Glacigene; deposited during the late Paleozoic glaciation. Outcrops are sparse in the Cobb Embayment and only identified with certainty at the western end; thickness in the embayment is unlikely to exceed 100 m. Maximum thickness of c. 2000 m in the Fitzroy Trough. Macrofossils and trace fossils are generally uncommon. Age constraint from palynology. Deposited under a variety of mainly non-marine glacial and periglacial siliciclastic environments, with local evidence of marine influence.|||Paterson Formation.|Unconformably underlain by Cobb Formation. Unconformably overlain by Samuel Formation and Bejah Claystone.|Typically grey to white sandstone, pebbly sandstone, conglomerate, mudstone and diamictite. Includes fine- to very coarse-grained, poorly sorted, pebbly and cobbly sandstone, interbedded with very poorly exposed mudstone.|
7696|Grant Group|73445|5|Briefly described|p3, 6, 8, 10, 12, 24, 65-118|Permian|Late Carboniferous|Canning Basin. Approximately 1300m of this unit's sediments overlie the Andrews Formation in the Point Moody No. 1 drillhole.||||Overlies Andrews Formation. Is overlain unconformably by the Poole Sandstone.|Conglomerate (including polymictic glacigene conglomerate), sandstone, siltstone and lignite.|
7696|Grant Group|73574|5|Briefly described|p762|Sakmarian|Asselian|Northeast Pilbara Craton. Unconformably overlies granite-greenstone bedrock. Shallow marine to fluvial, and possibly partly glacial.||||Unconformably underlies Poole Sandstone|Cross-bedded fine to very coarse quartz sandstone, laminated micaceous sandstone, siltstone, mudstone and minor conglomerate, fossiliferous; contains wood fragments and is bioturbated in places.|
7742|Grebe Sandstone Member|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Eocene|Paleocene|100-270m thick.||Hibernia Formation|||Sandstone, minor marl and limestone.|
7742|Grebe Sandstone Member|41532|2|Defined|p308|early Eocene|Late Paleocene|||||||07-NOV-08
7742|Grebe Sandstone Member|42442|2|Defined|p30|Eocene early|Late Paleocene|Same as Grebe Sandstone Member, WA.||||||07-NOV-08
7742|Grebe Sandstone Member|43699|6|Mentioned|Fig.6,p10||Eocene|||||||
7742|Grebe Sandstone Member|43739|6|Mentioned|Fig.5,p38|||||||||
7742|Grebe Sandstone Member|49637|5|Briefly described|Fig. 3|Eocene|Eocene|Of the Hibernia Formation. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
7742|Grebe Sandstone Member|64695|6|Mentioned|p261 Fig.6|||See also reference to Grebe Sandstone (p270). Northern Bonaparte Basin.||||||
7742|Grebe Sandstone Member|65680|6|Mentioned|p709 Fig.2.|Lutetian|Lutetian|||Unit in Hibernia Formation.||||
7742|Grebe Sandstone Member|69452|5|Briefly described|p36:15|Paleogene|Paleogene|Bonaparte Basin.||Hibernia Formation.||||12-JUL-16
7742|Grebe Sandstone Member|70061|5|Briefly described|Regional geology; Figs.6-7, p6, p12|Eocene|Eocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2. Sealed by carbonates within the Hibernia Formation.||Hibernia Formation.|||Lowstand sandstones.|12-JUL-16
7766|Greenough Sandstone|23815|6|Mentioned|p291|Early Jurassic|Early Jurassic|Geological Province: Carnarvon Basin.||||||14-DEC-04
7766|Greenough Sandstone|23816|4|Described|p243|Early Jurassic|Early Jurassic|Geological Province: Perth Basin. Of the Chapman Group. Underlying unit: Kockatea Shale (disconformable). Overlying unit: Moonyoonooka Sandstone (disconformable). Max. thickness: 95 m.||||||
7766|Greenough Sandstone|30948|6|Mentioned|Map legend|Lias|Lias|||||||
7766|Greenough Sandstone|31561|6|Mentioned|p18|||See also P22||||||
7766|Greenough Sandstone|31706|6|Mentioned|p665|||Jurassic correlation chart||||||
7766|Greenough Sandstone|31910|6|Mentioned|p21|||||||||
7766|Greenough Sandstone|32648|6|Mentioned|p32|||Liassic||||||
7766|Greenough Sandstone|32649|4|Described|p24|||Table 1||||||
7766|Greenough Sandstone|33022|6|Mentioned|p259|||||||||
7766|Greenough Sandstone|33166|6|Mentioned|p63|||Refers Arkell & Playford (1954)||||||
7766|Greenough Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
7766|Greenough Sandstone|35282|6|Mentioned|Fig.2|||||||||
7766|Greenough Sandstone|36257|6|Mentioned|Table 2.1|||||||||
7766|Greenough Sandstone|36293|2|Defined|p140|Early Jurassic|Early Jurassic|||||||
7766|Greenough Sandstone|36890|3|Fully described|p242|||||||||
7766|Greenough Sandstone|44144|4|Described|p506 Tb.4-21, p515|Early Jurassic|Early Jurassic|Type Section: Moonyoonooka 28o47'04''S 114o48'03''E. 95m thick fluvial deposits.||Chapman Group||Disconformably overlies Kockatea Shale. Overlain by Moonyoonooka Sandstone conformably.|Mottled red and white, medium- to coarse-grained argillaceous sandstone; siltstone, shale, claystone and conglomerate lenses.|
7766|Greenough Sandstone|61811|4|Described|p21, p29, p31, p34, p63.|Jurassic|Jurassic|Mount Minchin area. Appeared to lie conformably over the Minchin Siltstone. Type section on Moonyoonooka property east of Geraldton is described; further details in Appendix 1. 19 m thick.||Lower unit in Chapman Group.||Conformably overlies Minchin Siltstone. Is overlain by Moonyoonooka Sandstone.|Multicoloured, poorly sorted and bedded, medium- to coarse-grained sandstone with minor conglomerate and claystone.|
7766|Greenough Sandstone|64635|5|Briefly described|p16 |||Type section on the Moonyoonooka property east of Geraldton.||Of the Chapman Group.||Overlain by the Moonyoonooka Sandstone.|Multicoloured, poorly sorted and bedded, and medium to coarse grained with minor conglomerate and claystone.|
7766|Greenough Sandstone|64769|5|Briefly described|p37, p37 Fig. 26, p131 Fig. 135, p131|Early Jurassic|Early Jurassic|Geological Province: Perth Basin. Partially weathered, coarse- to medium-grained, bedded sandstone. WA.||||||
7823|Grierson Member|23815|6|Mentioned|p296|Aptian|Neocomian|Of the Birdrong Sandstone.||||||14-DEC-04
7823|Grierson Member|36890|4|Described|p296|||||||||
7823|Grierson Member|39211|6|Mentioned|p58|||Partly older than Aptian||||||
7823|Grierson Member|41271|3|Fully described|p147|||||||||
7823|Grierson Member|42598|5|Briefly described|P 96|||||||||
7854|Guildford Formation|12759|5|Briefly described|p33 Fig.16|Quaternary|Quaternary|Defined Aurousseau and Budge (1921) as "Guildford Clays"; redefined as a Formation by Low (1971); redefined here as Guildford Clay. Shown as laterally equivalent to Bassendean and Gnangara Sands.||Of Kwinana Group.||||
7854|Guildford Formation|22820|6|Mentioned|p23|Quaternary|Quaternary|Part of the Quaternary deposits unconformably overlying the Cretaceous rocks of the southern Perth Basin, including Warbro Group units.||||||12-AUG-08
7854|Guildford Formation|23816|6|Mentioned|p256|Quaternary|Quaternary|Geological Province: Perth Basin.||||||
7854|Guildford Formation|24094|6|Mentioned|p275|||Geological Province: Perth Basin||||||16-MAR-05
7854|Guildford Formation|24160|5|Briefly described|p48-49, p88 fig 38, p94-95, p99-103|Quaternary|Quaternary|Type section is the West Guildford artesian bore, from the surface down to 32.99m. Vast areas of smectite clays are a potential resource for construction industry clays, at Wokalup and Benger.||||Unconformably overlies Kings Park Shale, Osborne Formation, and Leederville Formation.|Lenticular interbeds of sand, clay and conglomerate, and is partly calcareous.|
7854|Guildford Formation|24410|5|Briefly described|p39|Quaternary|Quaternary|Of the Kwinana Group. Lenticular beds of sand, clay, conglomerate, calcareous. Overlain by Bassendean Sand; uncon. overlies Kings Park Shale, and Osborne Formation or Leederville Fm.  Geological Province: Perth Basin.||||||24-NOV-09
7854|Guildford Formation|29382|6|Mentioned|Fig.13|||||||||
7854|Guildford Formation|29383|6|Mentioned|Table 3|||||||||
7854|Guildford Formation|29693|6|Mentioned|p41|||||||||
7854|Guildford Formation|30217|5|Briefly described|p21|||||||||
7854|Guildford Formation|30939|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|31896|2|Defined|p34|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|33044|4|Described|p57|||See also maps 3 and 4 and diags. 17 and 18.||||||14-FEB-08
7854|Guildford Formation|35041|6|Mentioned|p367|||||||||
7854|Guildford Formation|35058|6|Mentioned|p64|||||||||
7854|Guildford Formation|35638|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|36293|3|Fully described|p215|||||||||
7854|Guildford Formation|36890|6|Mentioned|p256|||||||||
7854|Guildford Formation|37017|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|37309|5|Briefly described|p16|||||||||
7854|Guildford Formation|38479|4|Described|p18|||||||||
7854|Guildford Formation|38777|4|Described|p30|||||||||
7854|Guildford Formation|38954|6|Mentioned|Table 1|||||||||
7854|Guildford Formation|39554|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|39829|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|39915|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|40304|5|Briefly described|p42|||||||||
7854|Guildford Formation|40359|6|Mentioned|p28|||||||||
7854|Guildford Formation|40360|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
7854|Guildford Formation|40902|6|Mentioned|p55|||||||||
7854|Guildford Formation|41344|6|Mentioned|p11|||||||||
7854|Guildford Formation|41346|6|Mentioned|p9|||||||||
7854|Guildford Formation|41504|6|Mentioned|p71|||||||||
7854|Guildford Formation|41789|6|Mentioned|Fig.1|||||||||
7854|Guildford Formation|41986|4|Described|p38|||||||||
7854|Guildford Formation|42687|6|Mentioned|map legend|||||||||
7854|Guildford Formation|42688|6|Mentioned|map legend|||||||||
7854|Guildford Formation|43038|5|Briefly described|p17|||||||||
7854|Guildford Formation|43062|4|Described|p23,Table 2,p18|||||||||
7854|Guildford Formation|43066|5|Briefly described|Fig.2,p102|||||||||
7854|Guildford Formation|43096|5|Briefly described|p6|||||||||
7854|Guildford Formation|43189|5|Briefly described|Map Legend||Quaternary|||||||
7854|Guildford Formation|43212|5|Briefly described|p6||Pleistocene|||||||
7854|Guildford Formation|43304|5|Briefly described|Map Legend||Pleistocene|||||||
7854|Guildford Formation|43306|5|Briefly described|Map Legend||Quaternary|||||||
7854|Guildford Formation|43308|5|Briefly described|Map Legend||Quaternary|||||||
7854|Guildford Formation|43309|5|Briefly described|Map Legend||Quaternary|||||||
7854|Guildford Formation|43347|6|Mentioned|10|||||||||
7854|Guildford Formation|44144|4|Described|p502 Tb.4-21, p520 Fig.4-165|Pleistocene|Pleistocene|Type Section: West Guildford bore: 31o54'30''S 115o57'20''E. Up to 33m of fluvial sediments with estuarine and shallow marine incursions.||||Overlies Ascot Formation (disconformably), Kings Park Formation (unconformably).  Overlain by Muchea Limestone.|Lenticular interbeds of sand, clay and conglomerate; partly calcareous.|
7854|Guildford Formation|60556|5|Briefly described|p22, p24, p25 Fig. 15|||||||||
7854|Guildford Formation|63330|5|Briefly described|p192, p214|||Underlies the Pinjarra Plain of alluvial fans fronting the Darling Scarp and Darling Plateau. Clay, laterite, sand and muddy sand. Geological Province: Perth Basin/Swan Coastal Plain.||||||31-JAN-08
7854|Guildford Formation|63745|3|Fully described|p59, p61, p72||Early Pleistocene|Supersedes Guildford Clay. Unconformable on Ascot Fm; unconformable below Bassendean Sand; also below Perth Fm. Max. thick: 25m. Interfingers with Gnangara and Bassendean Sands. Clays+silts of alluvial fans. Max. thick: 27m. Underlies Pinjarra Plains.||||||07-FEB-11
7854|Guildford Formation|64769|6|Mentioned|p130 Fig. 133|Cenozoic|Cenozoic|||||||
7854|Guildford Formation|67135|5|Briefly described|p22, p30, p56.|||Clayey soils on this unit have swelled and shrunk with variation in water content, causing cracking in houses. Groundwater salinities are higher in areas underlain by these sediments. Has local deposits of lateritic gravel. Source of manufacturing clay near Bunbury.||||||
7854|Guildford Formation|68811|5|Briefly described|p90, p94|Quaternary|Neogene|One of a group of 'superficial sediments' described as being up to 90m thick. Referred to as the Guildford Clay (obsolete name) on p90.|||||Group description: Sand, limestone, silt and clay.|15-APR-20
7854|Guildford Formation|69081|6|Mentioned|p737 Fig.1|||Geol. Prov: Perth Basin||||||
7854|Guildford Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||estuarine, alluvial sediment|
7904|Gunga Meta-argillite|29784|6|Mentioned|Table 1|||||||||
7904|Gunga Meta-argillite|30632|6|Mentioned|p230|||||||||
7904|Gunga Meta-argillite|30900|6|Mentioned|p67|||On Table 1.||||||
7904|Gunga Meta-argillite|31042|6|Mentioned|Fig. 2|||||||||
7904|Gunga Meta-argillite|34324|6|Mentioned|p122|||Table||||||
7904|Gunga Meta-argillite|37373|6|Mentioned|Table 2.I|||||||||
7904|Gunga Meta-argillite|73391|6|Mentioned|Appendices.|||Glikson (1971). Regional stratigraphic correlation chart of other workers.|||||Argillite, slate, graphitic slate (no sandstones), minor BIF, intercalated basic igneous rocks.|
7922|Gurgadi Basalt|30388|4|Described|Table 1|||Middle Proterozoic age. Cassidy Group.||||||
7922|Gurgadi Basalt|30390|4|Described|p75|||See also p76||||||21-NOV-13
7922|Gurgadi Basalt|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7922|Gurgadi Basalt|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
7922|Gurgadi Basalt|36551|6|Mentioned|Table 31|||||||||
7922|Gurgadi Basalt|36886|4|Described|p198|||||||||
7922|Gurgadi Basalt|67244|5|Briefly described|Map legend.|||Bentley Basin. Shown only in the Interpreted Bedrock Geology section of the map sheet.||Unit in Cassidy Group.|||Basalt with vesicular and amygdaloidal flow tops; epidotized.|11-APR-12
7922|Gurgadi Basalt|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||<1065 Ma.|Unit in Cassidy Group.|||Basalt with vesicular and amygdaloidal flow tops; epidotized.|
7922|Gurgadi Basalt|67375|5|Briefly described|p20 Fig.11, p38 Table 1.|Mesoproterozoic|Mesoproterozoic|Thickness approximately 500-600 m.|1065-1057 Ma.|||Overlies Gombugurra Rhyolite, Wururu Rhyolite or, locally, Glyde Formation.|A succession of amygdaloidal basaltic lavas which contain numerous thin and laterally discontinuous layers, and small successions of volcaniclastic, cherty-epidotitic mudstones, siltstones, sandstones and conglomerates.|
7922|Gurgadi Basalt|67553|4|Described|p21,40,51,94|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin. Thickness: 500-600m including interbedded sedimentary rocks. Age constrained by 1065+\-5 Ma Wururu Rhyolite and 1057+\-6 Ma Thomas Rhyolite. ||Unit of Cassidy Group.||Overlain by Thomas Rhyolite. Underlain by Gombugurra Rhyolite.|Amygdaloidal basaltic lavas, which contain numerous, but thin and laterally discontinuous, layers, and small successions of volcaniclastic sedimentary rocks comprising cherty-epidotitic mudstones, siltstones, sandstones, and conglomerates.|
7922|Gurgadi Basalt|68995|5|Briefly described|p7 Fig.3, p9 Tb. 1, p18, p49 Fig.25|Stenian|Stenian|Estimated 600m thick.||Cassidy Group||Overlies the Gombugurra Rhyolite or the Wururu Rhyolite. Overlain by the Thomas Rhyolite.|Amygdaloidal basaltic lava flows with numerous thin and laterally discontinuous layers of volcaniclastic sedimentary rocks such as mudstones, siltstones, sandstones and conglomerates.|
7922|Gurgadi Basalt|69091|6|Mentioned|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
7922|Gurgadi Basalt|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Mentioned in GEOCHRON/174691.1.pdf and 174690.1.pdf.||Cassidy Group|||Basalt; epidotized; sample description includes: bluish-green dolerite-like rock possibly representing a massive and slightly coarser-grained effusive metabasalt; meta-igneous mafic volcanic, metabasalt|
7922|Gurgadi Basalt|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
7922|Gurgadi Basalt|70095|5|Briefly described|p16-17|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of basaltic package: 0.5km.||Unit of Cassidy Group.||Overlain by Thomas Rhyolite. Underlain by Gombugurra Rhyolite.||
7922|Gurgadi Basalt|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic||1047 Ma - 1077 Ma (Inferred)|Cassidy Group|||Basalt with vesicular and amygdaloidal flow tops; epidotized|
7922|Gurgadi Basalt|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Basalt with vesicular and amygdaloidal flow tops; epidotized|
7922|Gurgadi Basalt|71211|6|Mentioned|p216|||||Cassidy Group||||
7922|Gurgadi Basalt|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Basalt with vesicular and amygdaloidal flow tops; epidotized|
7922|Gurgadi Basalt|72443|6|Mentioned|p738-739, p747-748|||Talbot Sub-basin.||Cassidy Group||||
7936|Gwalia Slate|41677|6|Mentioned|p112|||||||||
7936|Gwalia Slate|42328|6|Mentioned|p1563|||||||||
7999|Hamelin Coquina|11797|5|Briefly described|map legend|Holocene|Holocene||||||Beach ridges, coquina of small Fragum erugatum shells.|
7999|Hamelin Coquina|35105|6|Mentioned|p42|||||||||
7999|Hamelin Coquina|38485|4|Described|p21|||||||||
7999|Hamelin Coquina|40342|6|Mentioned|Map legend|Holocene|Holocene|||||||
7999|Hamelin Coquina|40343|5|Briefly described|p14|||||||||
7999|Hamelin Coquina|41271|4|Described|p198|||||||||
7999|Hamelin Coquina|69558|4|Described|p2, p20, p24, p114, p116, p146, p151, |Holocene|Holocene|The oldest part of this unit is only 5316+/-42  years BP based on radiocarbon dating. Formed as a result of storms and cyclones crossing Hamelin Pool and L'Haridon Bight. Ridges dip towards the sea and show pronounced cyclicity. Up to 75m thick. See also p152, p155, p159, p163 fig 250, p170, p171, p187 fig 289, p229 fig 367, p230 fig 368, p234-p239, p246, p261, p265.|||||Beach ridges and mounds of Fragum erugatum shells, loose at shorelines and dominantly progressively cemented to coquinite away from coast..|25-MAY-21
8005|Hamersley Group|22475|6|Mentioned|Fig.1, Fig.4|||||||||
8005|Hamersley Group|22617|6|Mentioned|p675|||||||||
8005|Hamersley Group|22689|6|Mentioned|137,141 fig 2|||Geological province: Hamersley Basin. Of the Mount Bruce Supergroup.||||||16-JAN-07
8005|Hamersley Group|22715|6|Mentioned|fig7p212|||Coupled with Turee Creek Group on map legend.||||||
8005|Hamersley Group|22716|5|Briefly described|table4 p227|Paleoproterozoic|Archean|Underlain by Fortesque Group. Upper part deposited between 2470-2440ma.||||||07-NOV-08
8005|Hamersley Group|22814|6|Mentioned|p258|||||||||
8005|Hamersley Group|23045|5|Briefly described|289|||Max  thickness: 2400 m.||||||16-JAN-07
8005|Hamersley Group|23046|5|Briefly described|166|||Underlain by Fortescue Group.||||||16-JAN-07
8005|Hamersley Group|23047|5|Briefly described|34|||Hamersley Province. Of the Mount Bruce Supergroup. Underlain by Fortescue Group.||||||16-JAN-07
8005|Hamersley Group|23126|5|Briefly described|p381|||||||||
8005|Hamersley Group|23127|5|Briefly described|p376|||||||||
8005|Hamersley Group|23194|5|Briefly described|p41|Proterozoic|Archean|In the Hamersley Province.||||||07-NOV-08
8005|Hamersley Group|23205|6|Mentioned|p384, Fig.1|||||||||
8005|Hamersley Group|23280|5|Briefly described|p1084,Fig1p1085|||||||||
8005|Hamersley Group|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Mount Bruce Supergroup.||||||
8005|Hamersley Group|23354|5|Briefly described|315|||||||||
8005|Hamersley Group|23536|4|Described|p 427|||Also see Fig 2 p 429.||||||
8005|Hamersley Group|23570|5|Briefly described|p12|Archean|Archean|Thickness: ~2500m.   Geological Province: Pilbara Craton||||||07-NOV-08
8005|Hamersley Group|23575|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Underlain by Fortescue Group.||||||07-NOV-08
8005|Hamersley Group|23583|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23585|5|Briefly described|p19|Archean|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23594|4|Described|p17|Mesoproterozoic|Paleoproterozoic|Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23598|5|Briefly described|p13|||||||||
8005|Hamersley Group|23612|5|Briefly described|p840|||Geological Province: Hamersley Basin.  Max. thickness: 2500 m.||||||
8005|Hamersley Group|23745|5|Briefly described|p14||Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23746|5|Briefly described|p20|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23774|6|Mentioned|p733 table 1|||Of Mount Bruce Supergroup.||||||
8005|Hamersley Group|23870|6|Mentioned|p224 Fig. 1||Archean|Of Mount Bruce Supergroup.||||||07-NOV-08
8005|Hamersley Group|23890|4|Described|p9|Paleoproterozoic|Archean|Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|23936|4|Described|p3, Tb.1|Paleoproterozoic|Archean|Age: c.2.47 Ga. Geological Province: Hamersley Province. Underlain by Fortescue Group (unconformably).||||||01-MAR-10
8005|Hamersley Group|24025|5|Briefly described|p14|Paleoproterozoic|Archean|Of Mount Bruce Supergroup.  Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|24041|5|Briefly described|p493 fig.2|Paleoproterozoic|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Mount Bruce Supergroup.   Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|24169|5|Briefly described|p666 Fig. 5|||||||||
8005|Hamersley Group|24183|6|Mentioned|p2 Fig.1, p20|Paleoproterozoic|Archean|Unconformably overlain by the Collier Group.||||||07-NOV-08
8005|Hamersley Group|24185|5|Briefly described|p750|Siderian|Archean|Age: ca. 2450 Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|24188|5|Briefly described|p789 Fig.2, p799|Archean|Archean|Geological Province: Hamersley Basin||||||07-NOV-08
8005|Hamersley Group|24203|5|Briefly described|p292 Fig. 7|||Age: 2600-2500 Ma.   Geological Province Carnarvon Basin.||||||
8005|Hamersley Group|24231|5|Briefly described|p185, p186 Fig.2|Proterozoic|Proterozoic|Maximum thickness: 2500m.  Geological Province: Hamersley Basin.||||||
8005|Hamersley Group|24391|6|Mentioned|p8-2 Fig.1|Archean|Archean|Geological Province: Pilbara Block.||||||07-NOV-08
8005|Hamersley Group|24426|4|Described|Fig. 1, p217, p218|Paleoproterozoic|Archean|Thickness: 2.5 km. BIF, shale, carbonates and volcanics deposited in a marine environment. Age: 2600-2450 Ma. Geological Province: Hamersley Province.||||||07-FEB-11
8005|Hamersley Group|24533|5|Briefly described|p11, p4 Table 1.|Archean|Archean|Age of lower part: c.2600-2500Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|24534|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup.  Age: c.2595Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|24541|4|Described|p1, p11 Tb.2, p57|Paleoproterozoic|Neoarchean|Conformably or disconformably underlain by the Fortescue Group.||||||07-NOV-08
8005|Hamersley Group|24543|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Bruce Supergroup.  Age: c.2490Ma.||||||07-NOV-08
8005|Hamersley Group|24544|4|Described|p1, 54|Paleoproterozoic|Paleoproterozoic|Of Mount Bruce Supergroup. Overlies Fortescue Group. Conformably overlain by Turee Creek Group. Banded iron-formation, volcanic derived shale, chert, dolomite, and rhyolite are dominant lithologies. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|24573|6|Mentioned|p671 Fig.2|||Geological Province: Pilbara Craton||||||
8005|Hamersley Group|24602|5|Briefly described|p854 Fig. 1|Paleoproterozoic|Archean|Age: 3.0 - 2.4 Ga.||||||07-NOV-08
8005|Hamersley Group|24607|5|Briefly described|p967, 968, 969|Paleoproterozoic|Archean|Includes volcanic units ranging in age: 2597-2449 Ma. Geological Province: Hamersley Basin, Pilbara Craton.||||||30-NOV-10
8005|Hamersley Group|29358|6|Mentioned|p944|||||||||
8005|Hamersley Group|29596|5|Briefly described|Fig.2|||||||||
8005|Hamersley Group|29629|5|Briefly described|p899|||||||||
8005|Hamersley Group|29692|6|Mentioned|p203|||||||||
8005|Hamersley Group|29716|4|Described|Table 1|||||||||
8005|Hamersley Group|29717|6|Mentioned|p1153|||||||||
8005|Hamersley Group|29848|6|Mentioned|p413|||||||||
8005|Hamersley Group|30364|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|30437|6|Mentioned|p89|||Contains numerous banded iron formation units||||||
8005|Hamersley Group|30484|6|Mentioned|Fig.29|||||||||
8005|Hamersley Group|30488|6|Mentioned|p82|||||||||
8005|Hamersley Group|30490|6|Mentioned|p108|||||||||
8005|Hamersley Group|30685|6|Mentioned|p907|||||||||
8005|Hamersley Group|30766|6|Mentioned|p11|||||||||
8005|Hamersley Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
8005|Hamersley Group|30881|6|Mentioned|p527|||||||||
8005|Hamersley Group|30884|6|Mentioned|p159|||||||||
8005|Hamersley Group|31021|6|Mentioned|p893|||||||||
8005|Hamersley Group|31034|6|Mentioned|p134|||||||||
8005|Hamersley Group|31099|6|Mentioned|p41|||Phosphorus content. Refers Trendall and Blackley (1970)||||||16-JAN-07
8005|Hamersley Group|31154|6|Mentioned|p71|||||||||
8005|Hamersley Group|31311|6|Mentioned|p62|||re age dates||||||
8005|Hamersley Group|31393|6|Mentioned|Pl.25|||||||||
8005|Hamersley Group|31670|4|Described|p911|||||||||
8005|Hamersley Group|31819|6|Mentioned|p80|||Part of Mt. Bruce Supergroup||||||
8005|Hamersley Group|31828|5|Briefly described|p37|||Proterozoic, map. See also iron p41.||||||16-JAN-07
8005|Hamersley Group|31876|6|Mentioned|p11|||||||||
8005|Hamersley Group|31931|6|Mentioned|p81|||||||||
8005|Hamersley Group|32144|6|Mentioned|p116|||Organic matter||||||
8005|Hamersley Group|32326|5|Briefly described|p122|||Refers MacLeod et al (1963)||||||
8005|Hamersley Group|32389|6|Mentioned|p925|||||||||
8005|Hamersley Group|32722|6|Mentioned|Fig.2|||Stromatolite||||||
8005|Hamersley Group|32727|6|Mentioned|Fig.17|||||||||
8005|Hamersley Group|33537|4|Described|p109|||Breccia horizons discussed. See also pp110 - 112.||||||16-JAN-07
8005|Hamersley Group|33538|3|Fully described|p288|||See also pp289 - 294.||||||01-JUL-14
8005|Hamersley Group|33540|6|Mentioned|p885|||||||||
8005|Hamersley Group|33541|6|Mentioned|p103|||||||||
8005|Hamersley Group|33542|6|Mentioned|p411|||||||||
8005|Hamersley Group|33543|5|Briefly described|p132|||||||||
8005|Hamersley Group|33544|3|Fully described|p30|||See also pp31 - 41. Refers Macleod et al. (1963)||||||16-JAN-07
8005|Hamersley Group|33545|5|Briefly described|p112|||||||||
8005|Hamersley Group|33630|6|Mentioned|Table 1|||||||||
8005|Hamersley Group|33687|6|Mentioned|p916|||||||||
8005|Hamersley Group|33843|6|Mentioned|p170|||Refers Trendall & Blockley (1970)||||||
8005|Hamersley Group|34066|5|Briefly described|p5|||L.Prot. See also p6.||||||16-JAN-07
8005|Hamersley Group|34115|6|Mentioned|p383|||Age: 2000 +- 100 my.||||||16-JAN-07
8005|Hamersley Group|34124|6|Mentioned|p6|||||||||
8005|Hamersley Group|34128|6|Mentioned|p17|||Proterozoic||||||
8005|Hamersley Group|34129|6|Mentioned|p57|||Proterozoic||||||
8005|Hamersley Group|34135|4|Described|Table 2|||See also pp5,7,11,19,24. Lower Proterozoic.||||||16-JAN-07
8005|Hamersley Group|34287|6|Mentioned|p32|||See also p55.||||||16-JAN-07
8005|Hamersley Group|34541|6|Mentioned|p53|||Precambrian. Plate 25||||||
8005|Hamersley Group|34542|6|Mentioned|p93|||Precambrian. Plate 25.||||||
8005|Hamersley Group|34721|6|Mentioned|p286|||||||||
8005|Hamersley Group|34834|6|Mentioned|p212|||||||||
8005|Hamersley Group|35052|5|Briefly described|Fig.2|||||||||
8005|Hamersley Group|35218|4|Described|p4|||||||||
8005|Hamersley Group|35260|4|Described|p7|||||||||
8005|Hamersley Group|35269|4|Described|p304|||||||||
8005|Hamersley Group|35299|6|Mentioned|p893|||||||||
8005|Hamersley Group|35539|6|Mentioned|p317|||In reference to phosphatic sediments||||||
8005|Hamersley Group|35949|6|Mentioned|Fig.8|||||||||
8005|Hamersley Group|35975|6|Mentioned|Fig.37|||||||||
8005|Hamersley Group|35976|6|Mentioned|p107|||Also mentioned throughout paper.||||||
8005|Hamersley Group|36003|5|Briefly described|p1027|||||||||
8005|Hamersley Group|36004|6|Mentioned|p1089|||||||||
8005|Hamersley Group|36091|4|Described|p572|||||||||
8005|Hamersley Group|36247|4|Described|p186|||See also Fig.2.||||||
8005|Hamersley Group|36257|6|Mentioned|p29|||||||||
8005|Hamersley Group|36551|6|Mentioned|Table 23|||||||||
8005|Hamersley Group|36642|6|Mentioned|Table 1|||||||||
8005|Hamersley Group|36751|6|Mentioned|p473|||||||||
8005|Hamersley Group|36880|6|Mentioned|p108|||||||||
8005|Hamersley Group|36882|3|Fully described|p129|||||||||
8005|Hamersley Group|36884|6|Mentioned|p156|||||||||
8005|Hamersley Group|36891|5|Briefly described|p440|||||||||
8005|Hamersley Group|36902|6|Mentioned|p13|||||||||
8005|Hamersley Group|37170|5|Briefly described|p195|||||||||
8005|Hamersley Group|37212|6|Mentioned|p10|||||||||
8005|Hamersley Group|37297|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|37299|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|37327|6|Mentioned|p389|||||||||
8005|Hamersley Group|37371|6|Mentioned|p363|||||||||
8005|Hamersley Group|37460|3|Fully described|p113|||||||||
8005|Hamersley Group|37461|6|Mentioned|p321|||||||||
8005|Hamersley Group|37577|6|Mentioned|p6|||||||||
8005|Hamersley Group|37704|6|Mentioned|p507|||||||||
8005|Hamersley Group|37708|6|Mentioned|p1930|||||||||
8005|Hamersley Group|37934|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|38102|6|Mentioned|p189|||||||||
8005|Hamersley Group|38243|6|Mentioned|Fig.2|||||||||
8005|Hamersley Group|38321|6|Mentioned|Table 1|||||||||
8005|Hamersley Group|38482|6|Mentioned|p23|||||||||
8005|Hamersley Group|38496|5|Briefly described|p37|||||||||
8005|Hamersley Group|38768|6|Mentioned|p81|||||||||
8005|Hamersley Group|38776|5|Briefly described|Table 1|||||||||
8005|Hamersley Group|38790|4|Described|p161|||||||||
8005|Hamersley Group|38988|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|39171|6|Mentioned|p80|||||||||
8005|Hamersley Group|39200|4|Described|p281|||||||||
8005|Hamersley Group|39210|3|Fully described|p43|||See also Table 1.||||||24-JUL-07
8005|Hamersley Group|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8005|Hamersley Group|39426|4|Described|p12|||||||||
8005|Hamersley Group|39558|6|Mentioned|p256|||||||||
8005|Hamersley Group|39589|6|Mentioned|p157|||||||||
8005|Hamersley Group|39697|4|Described|p124|||||||||
8005|Hamersley Group|39894|6|Mentioned|p48|||||||||
8005|Hamersley Group|39952|5|Briefly described|p289|||||||||
8005|Hamersley Group|40089|6|Mentioned|p42|||||||||
8005|Hamersley Group|40103|6|Mentioned|p197|||||||||
8005|Hamersley Group|40109|5|Briefly described|p323|||||||||
8005|Hamersley Group|40369|6|Mentioned|p1|||||||||
8005|Hamersley Group|40448|5|Briefly described|p30|||[Originally entered for SA. CEBMar95]||||||
8005|Hamersley Group|40554|6|Mentioned|p29|||||||||
8005|Hamersley Group|40790|6|Mentioned|p192|||||||||
8005|Hamersley Group|40839|6|Mentioned|Fig.1|||||||||
8005|Hamersley Group|40852|5|Briefly described|p22|||||||||
8005|Hamersley Group|40854|6|Mentioned|p365|||||||||
8005|Hamersley Group|40904|6|Mentioned|p85|||||||||
8005|Hamersley Group|40905|6|Mentioned|p70|||||||||
8005|Hamersley Group|40937|5|Briefly described|p2|||||||||
8005|Hamersley Group|40938|6|Mentioned|p8|||||||||
8005|Hamersley Group|40987|6|Mentioned|Table 2|||||||||
8005|Hamersley Group|41125|6|Mentioned|p28|||||||||
8005|Hamersley Group|41349|6|Mentioned|p2|||||||||
8005|Hamersley Group|41351|6|Mentioned|Fig.2|||||||||
8005|Hamersley Group|41357|6|Mentioned|p123|||||||||
8005|Hamersley Group|41358|4|Described|p144|||||||||
8005|Hamersley Group|41592|6|Mentioned|p12|||||||||
8005|Hamersley Group|41622|6|Mentioned|p269|||||||||
8005|Hamersley Group|41635|6|Mentioned|Table 2|||||||||
8005|Hamersley Group|41669|5|Briefly described|p27|||||||||
8005|Hamersley Group|41768|4|Described|p26|||See also p21.||||||16-JAN-07
8005|Hamersley Group|41843|5|Briefly described|p67|||||||||
8005|Hamersley Group|41845|6|Mentioned|p81|||||||||
8005|Hamersley Group|41846|6|Mentioned|p97|||||||||
8005|Hamersley Group|41847|6|Mentioned|p104|||||||||
8005|Hamersley Group|41912|5|Briefly described|p20|||||||||
8005|Hamersley Group|41935|6|Mentioned|p12|||||||||
8005|Hamersley Group|41955|6|Mentioned|Fig.1 P4|||||||||
8005|Hamersley Group|41957|5|Briefly described|p67|||||||||
8005|Hamersley Group|41971|6|Mentioned|Fig.1 P342|||||||||
8005|Hamersley Group|42013|5|Briefly described|Map Legend|Proterozoic||||||||
8005|Hamersley Group|42112|4|Described|p8|||||||||
8005|Hamersley Group|42148|5|Briefly described|p685|||See also Table 1||||||
8005|Hamersley Group|42190|5|Briefly described|p274|||||||||
8005|Hamersley Group|42260|5|Briefly described|p6|||||||||
8005|Hamersley Group|42277|5|Briefly described|p63|||||||||
8005|Hamersley Group|42352|6|Mentioned|p4|||||||||
8005|Hamersley Group|42435|6|Mentioned|Fig.1 P43|||||||||
8005|Hamersley Group|42471|5|Briefly described|p7|||||||||
8005|Hamersley Group|42495|5|Briefly described|p2|||||||||
8005|Hamersley Group|42686|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
8005|Hamersley Group|42704|5|Briefly described|Plate 1 and Plate 2E|Proterozoic|Archean|Comprises Marra Mamba Iron Formation, Mount McRae Shale, Mount Sylvia Fm., Wittenoom Dolomite, brockman Iron Formation, Weeli Wolli Fm., Woongarra Volcanics and Boolgeeda iron Formation. Age: 2500Ma.||||||07-NOV-08
8005|Hamersley Group|42730|5|Briefly described|p12|||||||||
8005|Hamersley Group|42743|5|Briefly described|map legend|Proterozoic|Archean|||||||07-NOV-08
8005|Hamersley Group|42744|5|Briefly described|p4|||||||||
8005|Hamersley Group|42785|5|Briefly described|p261, Fig.2 p263|||Of Mount Bruce Supergroup.||||||16-JAN-07
8005|Hamersley Group|42898|5|Briefly described|Fig.2 P341|||Of the Mount Bruce Supergroup.||||||16-JAN-07
8005|Hamersley Group|43037|5|Briefly described|p24|||Of the Mount Bruce Supergroup.||||||16-JAN-07
8005|Hamersley Group|43052|5|Briefly described|Fig.3.8|||||||||
8005|Hamersley Group|43055|5|Briefly described|p17, Table 4|||||||||
8005|Hamersley Group|43056|5|Briefly described|Map Legend|||Of the Mount Bruce Supergroup.||||||22-DEC-09
8005|Hamersley Group|43063|5|Briefly described|Fig.1,p48|||||||||
8005|Hamersley Group|43064|5|Briefly described|p65|||||||||
8005|Hamersley Group|43119|5|Briefly described|p9|||||||||
8005|Hamersley Group|43210|5|Briefly described|Table1 p3,p4.|Paleoproterozoic|Archean|||||||07-NOV-08
8005|Hamersley Group|43262|5|Briefly described|Map Legend|Proterozoic|Archean|||||||07-NOV-08
8005|Hamersley Group|43290|5|Briefly described|p6||Archean|Of the Mount Bruce Supergroup.||||||07-NOV-08
8005|Hamersley Group|43561|6|Mentioned|p1433|||Age: approx. 2500-2400 Ma.||||||16-JAN-07
8005|Hamersley Group|43595|5|Briefly described|p73,75|Paleoproterozoic|Archean|Age: approx. 2.5 Ga (late Arch.-Early Prot.)||||||07-NOV-08
8005|Hamersley Group|43644|6|Mentioned|p594|||||||||
8005|Hamersley Group|43756|6|Mentioned|Fig.1,p534|||||||||
8005|Hamersley Group|44141|6|Mentioned|p304|||||||Is overlain unconformably by Bresnahan Group.||
8005|Hamersley Group|44142|6|Mentioned|p323|||||||Is overlain unconformably by Coondoon Formation (Manganese Subgroup).||
8005|Hamersley Group|44151|5|Briefly described|p158, p160 Fig.2-146||||c.2500 Ma (zircon U-Pb; Compston et al., 1981).|||Overlies Fortescue Group.||
8005|Hamersley Group|44152|4|Described|p163-164, p169 Fig.2-151, p173-174|||See also p176 Fig.2-154, p178-188. MacLeod et al. (1963). The "shale" may not be terrigenous clay or mud; rather a variant iron-formation.||Mount Bruce Supergroup|Marra Mamba, Brockman and Boolgeeda, Iron Formations; Wittenoom Dolomite; Mount Sylvia, Weeli Wolli Formations; Mount McRae Shale; Woongarra Volcanics.|Conformably overlies Fortescue Group. Is overlain conformably by Turee Creek Group.|Includes BIF, shale, subordinate carbonate; acid and basic intrusive rocks (dolerite sills, dacite and rhyolite sheets) constitute ~40% of total thickness.|
8005|Hamersley Group|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8005|Hamersley Group|44443|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8005|Hamersley Group|44477|4|Described|p.10-11, Table 1||Proterozoic|SF/50-6.||||||
8005|Hamersley Group|44478|14|Not recorded|map legend||Proterozoic|||||||
8005|Hamersley Group|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
8005|Hamersley Group|44501|14|Not recorded|p.6,11,12,13, map||Paleoproterozoic|Early Proterozoic. (F50-7). (ref. to MacLeod et al 1963).||||||07-NOV-08
8005|Hamersley Group|44502|14|Not recorded|map legend||Proterozoic|||||||
8005|Hamersley Group|44503|4|Described|p.5,8,12, Tb.2, map|||Roy Hill Sheet. (F50-12). See also p.17,20, for more details.||||||
8005|Hamersley Group|44692|4|Described|p.6,7,11,Tb.1, map|||See also p.13,15,17,19,23,25, for more details. (F50-11).||||||
8005|Hamersley Group|44729|5|Briefly described|map legend|Proterozoic||Of Mount Bruce Supergroup.||||||
8005|Hamersley Group|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8005|Hamersley Group|44867|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
8005|Hamersley Group|45086|4|Described|p22|||Age. Lithology. Iron ore deposits.||||||
8005|Hamersley Group|46319|4|Described|p14|Paleoproterozoic|Paleoproterozoic|Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|46899|6|Mentioned|p8|||||||||
8005|Hamersley Group|46917|6|Mentioned|p172|||||||||
8005|Hamersley Group|50131|6|Mentioned|p3|Early Proterozoic|Archaean|Of Mount Bruce Supergroup. Includes Marra Mamba Iron Formation. Geological Province: Pilbara Craton.||||||22-APR-09
8005|Hamersley Group|50216|5|Briefly described|p209|Paleoproterozoic|Archean|Comprises carbonates, shale and banded-iron-formation with bimodal volcanic rocks and intrusions in the upper units. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|50217|5|Briefly described|p220, p221 Fig.1|Paleoproterozoic|Archean|Age: 2597-2449 Ma. (Barley et al, 1997; Trendall et al, 1998; Nelson et al, 1999). Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|50225|5|Briefly described|p386 Fig. 1|||||||||07-FEB-11
8005|Hamersley Group|50226|6|Mentioned|p415|||||||||
8005|Hamersley Group|50227|5|Briefly described|p442, p443 Fig. 1|Mesoproterozoic|Paleoproterozoic|Age: 2600-2439Ma.  Geological Province: Hamersley Province.||||||07-FEB-11
8005|Hamersley Group|50287|5|Briefly described|Map Legend|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|50382|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mount Bruce Supergroup. Geological Province: Hamersley Basin, Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|50544|5|Briefly described|p51-52, p10 Fig. 5||Archean|Of the Mount Bruce Supergroup.  Represented solely by the Carawine Dolomite on YARRIE.  Age: c.2541Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|50549|5|Briefly described|p1158|Paleoproterozoic|Archean|Of the Mount Bruce Supergroup. Some of world's largest iron ore deposits in Dales Gorge Member.||||||07-NOV-08
8005|Hamersley Group|50555|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Includes the Carawine Dolomite.  Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|60373|4|Described|p145 Tb. 1|Archean|Archean|Of Mount Bruce Supersequence. Includes eight formations. Geological Province: Hamersley Province.||||||23-JUN-09
8005|Hamersley Group|60429|6|Mentioned|p25|||||||||07-FEB-11
8005|Hamersley Group|60539|5|Briefly described|p498 Fig.1|Paleoproterozoic|Archean|Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|60706|5|Briefly described|p622|Paleoproterozoic|Archean|Middle unit of the Mount Bruce Supergroup. Conformably overlies the Fortescue Group; conformably underlies the Turee Creek Group. Age: ~2449+/-3Ma (SHRIMP). Max. thickness: ~2.5 km. Contains BIF units up to 360m thick. Geological Province: Hamersley Basin||||||07-NOV-08
8005|Hamersley Group|61254|6|Mentioned|p257 Fig.1, p258 Fig.2|Neoarchean|Neoarchean||||Includes Marra Mamba Iron Formation.|Overlies Fortescue Group.||
8005|Hamersley Group|61259|5|Briefly described|p404 Fig. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|61268|5|Briefly described|p78 Fig.1|||Of the Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||
8005|Hamersley Group|61276|6|Mentioned|p577 Fig.1|||||||||
8005|Hamersley Group|61556|6|Mentioned|p10|||Compared in the context of iron formations.||||||
8005|Hamersley Group|61575|5|Briefly described|p759|||Banded-iron formation and argillite, which in turn contain thin interbeds of carbonate and volcaniclastic rocks. Unconformably overlies Jeerinah Formation. Geol. Prov: Hamersley Basin.||||||
8005|Hamersley Group|61576|5|Briefly described|p773|||Of the Mount Bruce Supergroup. Geological Province: Hamersley Basin.||||||
8005|Hamersley Group|61847|5|Briefly described|p295|Paleoproterozoic|Paleoproterozoic|Includes: Marra Mamba iron Formation, Wittenoom Dolomite, McRae Shale, Brockman Iron Formation. Unconformably overlies the Fortescue Group. Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|61897|5|Briefly described|p8|||Includes the Marra Mamba Formation.  Banded-iron formation, macro-bands alternate with shale layers; the lower part of the group (Marra Mamba Formation) shows vertical facies variation.||||||05-JUN-06
8005|Hamersley Group|62094|5|Briefly described|p236 Fig. 1|||Geological Province: Pilbara Craton.||||||
8005|Hamersley Group|62129|4|Described|p2, p5, p13 Fig. 1, p23 Fig. 3|Proterozoic|Archaean|Of Mount Bruce Supergroup. Includes, Brockman Iron Formation, Marra Mumba Iron Formation. Geological Province: Hamersley Basin.  Iron formations.||||||07-FEB-11
8005|Hamersley Group|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes eight units. Geological Province: Hamersley Basin, Pilbara Craton.||||||23-MAR-09
8005|Hamersley Group|62579|5|Briefly described|p116|Archean|Archean|Of Mount Bruce Supergroup. Geological Province: Pilbara Craton.||||||07-NOV-08
8005|Hamersley Group|63139|5|Briefly described|p50|||Of the Mount Bruce Supergroup. In east Pilbara. Comprises dolomite, chert, banded iron formation, shales and felsic and mafic rocks.||||||29-MAR-07
8005|Hamersley Group|63153|4|Described|p1359-1360, p1363. |Paleoproterozoic|Archean|All minerals in this Group's BIF were recrystallised during diagenesis and metamorphism; there is no trace of original granules or terrigenous clastic material.|2.6-2.4 Ga (Trendall et al., 2004).|Of the Mount Bruce Supergroup.|Includes Marra Mamba, Brockman and Boolgeeda Iron Formations; Wittenoom, Mount Sylvia, Weeli Wolli Formations; Mount McRae Shale; Woongarra Volcanics.|Conformably overlies the Fortescue Group. Conformably overlain by the Turee Creek Group.|Predominantly chemical sedimentary rocks, with lesser ash-fall deposits and intrusions.|
8005|Hamersley Group|63245|6|Mentioned|p14|||Contains 2.5Ga kerogens.||||||
8005|Hamersley Group|63367|5|Briefly described|p230,p231 Fig.1, |||||Of the Mount Bruce Supergroup.|Includes Carawine Dolomite.|Overlies the Fortescue Group.||
8005|Hamersley Group|63372|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Geological Province: Hamersley Basin. Of the Mount Bruce Supergroup.||||||07-NOV-08
8005|Hamersley Group|63417|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Includes the Carawine Dolomite. Age: 2548-2541Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
8005|Hamersley Group|63432|5|Briefly described|p735, p736 Fig. 2|Proterozoic|Proterozoic|Includes the Weeli Wolli and Wittenoom Formations, Marra Mamba, Brockman and Boolgeeda Iron Formations, Mount McRae Shale and Mount Sylvia Formation, and Woongarra Volcanics. Geological Province: Hamersley Province.||||||07-FEB-11
8005|Hamersley Group|63866|5|Briefly described|p144, p154, p162|Paleoproterozoic|Archaean|Hamersley Basin.||Mount Bruce Supergroup||Conformably (transitionally) overlain by the Turee Creek Group. Unconformably overlain by the Collier Group.||
8005|Hamersley Group|64174|5|Briefly described|Map legend|Archean|Archean|Of the Mount Bruce Supergroup. Subdivided informally into upper and lower parts: upper banded-iron formation, chert, siltstone, shale, dolerite and rhyolite; lower carbonate rock with lesser siliciclastic sedimentary rocks, BIF and chert.||||||07-NOV-08
8005|Hamersley Group|64326|5|Briefly described|p70|Archean|Archean|Middle part of Mount Bruce  Supergroup. Geological province: Hamersley Basin.||||||07-FEB-11
8005|Hamersley Group|64384|4|Described|p25, p29, p36-40|Paleoproterozoic|Archean|Of Mount Bruce Supergroup. Contains Marra Mamba Fm., Wittenoom Dolomite, Mt Sylvia Fm., Mt McRae Shale, Brockman Iron Fm., Weeli Wolli Fm., Woongarra Volcanics+Boolgeeda Iron Fm. Age:c.2500Ma (Compston et al 1981). In Hamersley Basin. BIF-dominated rocks||||||07-FEB-11
8005|Hamersley Group|64573|5|Briefly described|p784|||Overlies Fortescue Group. Geological Province: Pilbara Craton. Shales and banded iron-formations.||||||07-FEB-11
8005|Hamersley Group|64580|4|Described|map legend|Paleoproterozoic|Neoarchean|Of Mount Bruce Supergroup. Banded iron-formation, chert, mudstone, siltstone, dolomite, rhyolite, and numerous dolerite sills; metamorphosed.||||||09-DEC-08
8005|Hamersley Group|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes Marra Mamba Iron Formation. Age: c. 2597Ma. Geological Province: Pilbara Craton (Hamersley Basin).||||||
8005|Hamersley Group|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Mount Bruce Supergroup. Includes Marra Mamba Iron Formation, Wittenoom Formation and Mount McRae Shale. Geological Province: Hamersley Basin.||||||
8005|Hamersley Group|64662|6|Mentioned|p44|Archean|Archean|Pilbara Craton. Possible source rocks for Ferdies Member, Dead Bullock Formation.||||||07-FEB-11
8005|Hamersley Group|64722|5|Briefly described|Fig. 2 p3-6 p7, 21, 23|Siderian|Neoarchean|Hamersley Basin succession from rifting of the Pilbara and Yilgarn cratons in the late Archean / early Proterozoic.||||Overlies Fortescue Group, overlain by Turee Creek Group.||11-APR-12
8005|Hamersley Group|64724|4|Described|p43, p42 Fig. 3|Paleoproterozoic|Neoarchean|Hamersley Basin.|||Contains Wittenoom, Mount Sylvia, Weeli Wolli Formations; Mount McRae Shale; Carawine Dolomite; Woongarra Volcanics; and Brockman, Boolgeeda and Marra Mamba Iron Formations.|||02-APR-12
8005|Hamersley Group|64725|5|Briefly described|p58 Fig.2, p59.|||Hamersley Basin. Covers about 40,000 km2; about 2.5 km thick.|c.2470-2450 Ma.||Includes Marra Mamba, Brockman, Boolgeeda Iron-formations; Wittenoom Dolomite; Mount Silvia, Weeli Wolli Formations; Mount McRae Shale; Woongarra Rhyolite.|||02-APR-12
8005|Hamersley Group|64728|6|Mentioned|p94 Fig.1, p97, p107.||||Depositional age from c.2629 Ma to 2449 Ma.|||Overlies Fortescue Group. Is overlain by Turee Creek Group.||
8005|Hamersley Group|64830|5|Briefly described|p1108|||Of Mount Bruce Supergroup. Geological province: Hamersley Basin.||||||05-FEB-09
8005|Hamersley Group|65194|5|Briefly described|p98 Fig.4.23, p107|Proterozoic|Proterozoic|Unit in Mount Bruce Supergroup. Misspelt as Hammersley on p107.||||||11-APR-16
8005|Hamersley Group|65506|6|Mentioned|p987 Fig.1A|||||||||
8005|Hamersley Group|65683|4|Described|p799, p800, p801 Fig2, p802|||Of Mount Bruce Supergroup. Includes Boolgeeda Iron Formation, Woongarra Volcanics, Weeli Wolli Formation, Brockman Iron Formation, Mount McRae Shale, Mount Sylvia Formation, Wittenoom Formation, Marra Mamba Iron Formation. Overlies Fortescue Group. Stratigraphy is remarkably uniform throughout its province; a sequence of chemical sedimentary rocks consisting of banded iron-formation, chert and carbonate with volcaniclastics but little or no terrigenous sedimentary material.||||||08-MAR-12
8005|Hamersley Group|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Mount Bruce Supergroup. Includes Carawine Dolomite. Geol. Prov: Hamersley Basin, Pilbara Craton.||||||
8005|Hamersley Group|65757|6|Mentioned|p81 Tb.2, p88|||In the Hamersley Basin. Includes Carawine Dolomite.||||||
8005|Hamersley Group|65825|4|Described|p1, p6, p20, p23. |Archean|Archean|Hamersley Basin. Deposition of its sediments is interpreted to have occurred on a thermally subsiding continental margin.||Unit in Mount Bruce Supergroup.|Includes Marra Mamba Iron Formation, Wittenoom Formation and Carawine Dolomite.|Conformably overlies Fortescue Group.|Banded iron-formation, ferruginous shale, and dolomite.|
8005|Hamersley Group|65827|6|Mentioned|p41|||||||||
8005|Hamersley Group|65828|6|Mentioned|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton.||Unit in Mount Bruce Supergroup.|Includes Carawine Dolomite.|||
8005|Hamersley Group|65829|5|Briefly described|p1, p7 Fig.3, pp23-26.|Neoarchean|Neoarchean|Exposure of this Group in the map area is solely of the Carawine Dolomite.||Unit in Mount Bruce Supergroup.|Includes Carawine Dolomite.|||
8005|Hamersley Group|66115|6|Mentioned|p137 Fig.1|||||||||
8005|Hamersley Group|66217|5|Briefly described|p44.|Neoarchean|Neoarchean|Hamersley Basin.|2630-2450 Ma.|Unit in Mount Bruce Supergroup.||Conformably overlies Fortescue Group.||
8005|Hamersley Group|66299|6|Mentioned|p292.|||Hosts iron ore deposits.||||||
8005|Hamersley Group|66574|5|Briefly described|p912, p918 Fig.6, p920 Fig.9|||Mount Bruce Supergoup. McGrath Trough, underlies the Turee Creek Group, overlies the Fortescue Group. Records conversion of rifted Pilbara Craton margin to a passive continental margin, c.2629 Ma. Includes Woongarra Rhyolite, Boolgeeda and Brockman Iron Formations, Weeli Wolli Formation.||||||
8005|Hamersley Group|66745|6|Mentioned|p50 Fig.1.|Neoarchean|Neoarchean|||Unit in Mount Bruce Supergroup.||||
8005|Hamersley Group|66882|5|Briefly described|p99, p118|Siderian|Neoarchean|Hamersley Basin, Pilbara Craton. Suggested correlation with BIF in Middleback Group suggests links between Pilbara and Gawler Cratons.|2630-2450 Ma||Includes Brockman Iron Formation, Jeerinah Formation, Mount Newman Member, Bee Gorge Member.||Contains BIF.|
8005|Hamersley Group|66887|5|Briefly described|p2, p20-21|||Pilbara Craton.|||Carawine Dolomite, Marra Mamba Iron Formation, Mount McRea Shale, Brockman Iron Formation, Weeli Wolli Formation, Woongarra Rhyolite|||
8005|Hamersley Group|67025|4|Described|pp317-328.|Paleoproterozoic|Archean|Hamersley Basin, Pilbara Block. 2.5 km thick sequence of sedimentary and volcanic rocks including large hematite-goethite iron deposits within BIFs. The natural remanent magnetisation and mean bulk susceptibility of units in this Group are detailed in this article. There exists a regional remanent magnetic overprint directed moderately upwards to the northwest.|2629 - 2449 Ma (Trendall et al. 2004).|Unit in Mount Bruce Supergroup.|Includes Marra Mamba, Brockman and Boolgeeda Iron Formations; Wittenoom Dolomite; Mount Sylvia and Weeli Wolli Formations; Mount McRae Shale; Woongarra Volcanics.|Conformably overlies Fortescue Group. Is conformably overlain by Turee Creek Group.|Four important iron formations separated by sequences of dolomite, shales and volcanics.|
8005|Hamersley Group|67056|4|Described|p419 Fig.2, pp422-423, p424, p446.|Paleoproterozoic|Archean|Thickness about 2.5 km. Hosts three economic BIF units; the Marra Mamba Iron Formation, and the Dales Gorge and Joffre Members of the Brockman Iron Formation.|c.2.63 - 2.45 Ga.|Unit in Mount Bruce Supergroup.|Includes Marra Mamba, Brockman and Boolgeeda Iron Formations; Woongarra Rhyolite; Mount Whaleback and Mount McRae Shales; Weeli Wolli, Mount Sylvia and Wittenoom Formations.|Conformably overlies Fortescue Group. Is overlain by Turee Creek Group. Intruded by dolerite dykes and sills, and the Woongarra Rhyolite.|Sequence of five major BIF units interspersed with a dolomitic unit and shales; minor cherts and BIF; terrestrial clastics very rare.|
8005|Hamersley Group|67130|5|Briefly described|p1, p5, p6, p24 fig 17|||Maximum total thickness of 2.5 km. Misspelt Hamesley Group (page 37). See also p31, p34 fig 29, p37, p40 fig 38.|2630 Ma - 2450 Ma|Mount Bruce Supergroup|Brockman Iron Formation, Wittenoom Formation, Marra Mamba Iron Formation, Mount Sylvia Formation, Mount McRae Shale, Woongarra Rhyolite, Boolgeeda Iron Formation, Weeli Wolli Formation|Conformably (and gradationally) overlies Fortescue Group, conformably overlain by Turee Creek Group|Thick succession of banded iron formation, interbedded with shale and carbonate rocks and a variety of intrusive and extrusive igneous rocks (up to 40% of the group)|
8005|Hamersley Group|67183|4|Described|p639,p642-4, p649 Fig.8, p651,p668, p671|Neoarchean|Neoarchean|In the southern Pilbara Craton this is a thick sequence of banded iron formations and lesser dolomite. Of the Oakover Basin (also known as the Oakover Syncline, Hickman 1978), eastern Pilbara Craton.|ca 2700-2450 Ma|Mount Bruce Supergroup|Carawine Dolomite, Pinjian Chert Breccia, Turee Creek Formation.|Conformably overlies the Fortescue Group.|Banded iron formation, dolomite, shale, chert.|
8005|Hamersley Group|67201|4|Described|p9 Fig.5, p19, p28, p32-36, see comments|||Pilbara Craton, Hamersley Basin. Unconformably overlies Kurrana Terrane. Thickness: ~2.5 km. Mostly 'deeper' marine-shelf deposits, deposited in sediment-starved basin or shelf, or otherwise on shelf platform; with exception of Carawine Dolomite and parts of Wittenoom Formation. Page location continued: p38, p53 Fig.40, p54.|||Marra Mamba Iron Formation, Wittenoom Formation, Mount Sylvia Formation, Mount McRae Shale, Brockman Iron Formation, Weeli Wolli Formation, Woongarra Rhyolite, Boolgeeda Iron Formation|Overlies Jeerinah Formation (Fortescue Group). Is apparently conformably overlain by Turee Creek Group.|BIF, argillite, carbonate, and fine-grained volcaniclastic rock.|24-NOV-16
8005|Hamersley Group|67202|5|Briefly described|p52, p119, p125, p258|Archean|Archean||||Carawine Dolomite, Pinjian Chert Breccia.|||
8005|Hamersley Group|67229|6|Mentioned|p2 Fig.1, p3|||Fortescue Basin, Pilbara region.||Mount Bruce Supergroup.||||
8005|Hamersley Group|67721|5|Briefly described|p36, p37, p38 Fig.9, p38|Neoarchean|Neoarchean|Contains successions of Banded iron formation and associated iron ore deposits.|c. 2630-2450 Ma|Of the Mount Bruce Supergroup.|Includes the Brockman iron formation, Boolgeeda iron formation, Woongarra Rhyolite, Wheeli Wolli Formation, Mount McRae Shale, Mount Sylvia Shale, Wittenoom Formation, Marra Mamba iron formation.|||
8005|Hamersley Group|67827|6|Mentioned|p415||||||Includes Marra Mamba Iron Formation.|||
8005|Hamersley Group|67829|5|Briefly described|pp453-454.|||Erosion and solution have removed immense tonnages of silica from these rocks since the Paleoproterozoic. The unit lacks suitable aquifers for solutions leaching silica from iron ore-rich units.||||||
8005|Hamersley Group|67843|6|Mentioned|p33.|||Hamersley Basin.||||||
8005|Hamersley Group|67855|5|Briefly described|p212, 210, 211, 223, 224 , 225|||Hamersley Basin.||Of Mount Bruce Supergroup.|Includes Woongarra Volcanics.|||
8005|Hamersley Group|68035|4|Described|p292, 283, 284 Fig 1,p286, 292|Paleoproterozoic|Neoarchean|Hamersley Basin.  Prior to 2007 included in Pilbara Craton, but now considered to overlie it.  In the S Pilbara,  is c. 2.5 km thick, lies conformably on rocks of the Fortescue Group, and includes four BIF-dominated formations, mostly separated by shales.|2.63 - 2.45 Ma||Includes Marra Mamba, Brockman, and Boolgeeda Iron Formations, and the Weeli Wolli & Mount Sylvia  Formations; also Wittenoom Formation, Woongarra Rhyolite.|Conformably overlies Fortescue Group. Overlain by Turee Creek Group.|Banded iron formation, shale, minor carbonate, rhyolite.|
8005|Hamersley Group|68056|6|Mentioned|p170-171, 185, 188, 190|Archean|Archean||||Marra Mamba Iron Formation.|Overlies Fortescue Group.||
8005|Hamersley Group|68101|6|Mentioned|p2 Fig.1|||||||||
8005|Hamersley Group|68141|6|Mentioned|p195|Archean|Archean|Pilbara Craton.|||Dales Gorge Member.|||
8005|Hamersley Group|68280|6|Mentioned|p1, p2 fig 1a, p3, p5|Paleoproterozoic|Neoarchean|See also p41, p48, p54, p56-p58, p61.|2630-2450 Ma||Includes Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation, Mount McRae Shale, Mount Sylvia Formation, Wittenoom Formation, Marra Mamba Iron Formation|||16-JAN-23
8005|Hamersley Group|68574|6|Mentioned|p2|||||||||
8005|Hamersley Group|68981|5|Briefly described|p21, p26|Paleoproterozoic|Archean|Pilbara Craton. Overlies Archean granite-greenstone terranes. Volcanic and sedimentary rocks. Detrital zircons discussed.||||||
8005|Hamersley Group|69003|5|Briefly described|p7, p9 Fig.9, p36|||During the 2215-2145 Ma Ophthalmia Orogeny, this unit was deformed, folded, and thrust northward over the Pilbara Craton to form the Ophthalmia Fold Belt.|||||Dolerite sill.|
8005|Hamersley Group|69028|5|Briefly described|Map Legend|Siderian|Neoarchean|Hamersley Basin. Geochronology by Barley et al. (1997), Pickard (2002), Rasmussen et al. (2005) and Trendall et al. (1998).|2630-2445 Ma.||Includes Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation, Mount McRae Shale, Mount Sylvia Formation, Wittenoom Formation, and Marra Mamba Iron Formation.||Includes mudstone, siltstone, sandstone, dolomite, banded iron-formation, chert, rhyolite, rhyodacite, rhyolitic breccia, and dolerite sills; metamorphosed.|07-MAY-14
8005|Hamersley Group|69080|4|Described|p684, p687-688, p690-699|Paleoproterozoic|Neoarchean|Hamersley Basin, Pilbara Craton. 2.5 to 3 km thick. Deposition in a rift setting, from passive continental margin to active margin.|c.2629-c.2445 Ma.||Marra Mamba, Brockman and Boolgeeda, Iron Formations; Wittenoom, Mount Sylvia and Weeli Wolli Formations; Mount McRae Shale.|Conformably overlies Fortescue Group.|Sandstone, shale, dolomite and BIF.|
8005|Hamersley Group|69166|6|Mentioned|500k_geologyp08_lut.csv|Neoarchean|Neoarchean||||Includes Wittenoom Formation, Marra Mamba Iron Formation, Brockman Iron Formation, Weeli Wolli Formation, Boolgeeda Iron Formation, Woongarra Rhyolite|||
8005|Hamersley Group|69167|6|Mentioned|geologyp_lut.csv|Neoarchean|Neoarchean|||Mount Bruce Supergroup|Includes Mount Mcrae Shale, Wittenoom Formation, Carawine Dolomite, Marra Mamba Iron Formation|||
8005|Hamersley Group|69185|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Neoarchean|Geological Province: Pilbara Craton. Of Hamersley Basin. Also includes Mount Sylvia Formation, Weeli Wolli Formation, Wittenoom Formation, Woongarra Rhyolite. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.||Unit of Mount Bruce Supergroup.|Includes Boolgeeda Iron Formation, Brockman Iron Formation, Carawine Dolomite, Marra Mamba Iron Formation, Mount McRae Shale.||Banded iron-formation, chert, mudstone, siltstone, dolomite, rhyolite, and numerous dolerite sills; metamorphosed|
8005|Hamersley Group|69267|6|Mentioned|p658||||||||Podding and pinch and swell structures are common in BIF.|
8005|Hamersley Group|69299|6|Mentioned|p20|||||Of Mount Bruce Supergroup.||||
8005|Hamersley Group|69301|5|Briefly described|p16-17, p21 Fig.8|||Fortescue Group is distinguished from Hamersley Group by three main eruption events of basaltic formations. Jeerinah Formation (upper part of Fortescue Group), is assigned to sequence 4, which also includes Hamersley Group.|2630-2450 Ma|Mount Bruce Supergroup||Conformably overlies Fortescue Group.||
8005|Hamersley Group|69387|6|Mentioned|p6|||Southern Pilbara Craton. Extension-rift fill sequence of siliciclastic sedimentary and volcanic rocks.||||||
8005|Hamersley Group|69538|5|Briefly described|p516 Fig.2, p517 Fig.3, p520, p534|Paleoproterozoic|Paleoproterozoic|See also p559 Fig.34, p579. ||Unit in Mount Bruce Supergroup.|Includes Marra Mamba, Brockman, Boolgeeda Iron Formations; Wittenoom, Mount Sylvia, Weeli Wolli Formations; Mount McRae Shale; Woongarra Rhyolite.|Overlies Fortescue Group. Is overlain by Turee Creek Group.|Includes shallow-water reef limestones.|27-MAY-16
8005|Hamersley Group|69543|6|Mentioned|p87|||||||||
8005|Hamersley Group|69563|6|Mentioned|p689-690||||||Includes Wittenoom, Mount Sylvia, Weeli Wolli Formations; Brockman, Boolgeeda, Iron Formations; Mount McRae Shale; Woongarra Volcanics.|||
8005|Hamersley Group|69565|5|Briefly described|p131, p133 Fig.1, p139-140|||Hamersley Province.||Mount Bruce Supergroup.|Weeli Wolli Formation, Woongarra Rhyolite, Boolgeeda Iron Formation.|Overlies Fortescue Group. Is overlain conformably by Turee Creek Group.||
8005|Hamersley Group|69569|6|Mentioned|p285 Fig.1, p287-288|||East Pilbara Terrane. Three impact spherule layers have been found, dating to 2630 Ma, 2560-2500 Ma, and 2500-2480 Ma.|||Marra Mamba, Brockman, Iron Formations; Wittenoom, Mount McRae, Mount Sylvia, Boolgeeda, Weeli Wolli Formations.|||
8005|Hamersley Group|69590|5|Briefly described|GEOL_LUT_CSV files|||Of Hamersley Basin. See 100k_geologyp_lut.csv, 100k_geologyl_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv2_5m_geologyp98_lut.||Unit of Mount Bruce Supergroup.|Includes Boolgeeda Iron Formation, Brockman Iron Formation, Carawine Dolomite, Marra Mamba Iron Formation, Wittenoom Formation.|||
8005|Hamersley Group|69596|5|Briefly described|p1-2, p4-7, p8 Fig.5, p15, p17|Archean|Archean|Ophthalmia Fold Belt, Capricorn Orogen. About 3km thick. Passive margin deposition: deeper marine distal deposits.|2630-2450 Ma.|||Conformably overlies Fortescue Group.|Dominated by BIF, shale, chert and fine-grained carbonate; felsic volcanics.|
8005|Hamersley Group|69739|5|Briefly described|p68-70, 73|||Hamersley Basin. 2.5 km thick.|2.4 Ga.|Mount Bruce Supergroup.|Brockman Iron Formation, Wittenoom Formation, Marra Mamba Iron Formation.|Overlies Fortescue Group. Is overlain by Turee Creek Group.|Stratified sequence of BIF, shale, chert, dolomite and tuff. Numerous sills of dolerite and rhyolite up to 1km thick.|
8005|Hamersley Group|69745|5|Briefly described|p268-273, 275-276, 283, 287, 289|Proterozoic|Proterozoic|Hamersley Province. See also reference to Upper Hamersley Group (p269).||Mount Bruce Supergroup.|Marra Mamba, Brockman, Boolgeeda, Iron Formations; Wittenoom, Mount Sylvia, Mount McRae, Weeli Wolli, Woongarra Formations|Conformably overlies Fortescue Group. Is overlain conformably by Turee Creek Group.||
8005|Hamersley Group|69754|6|Mentioned|p314-p319, p330-p333, p339-p340|||Hamersley Basin.||||Conformably overlain by the Kungarra Formation (Turee Creek Group).|Banded-iron formation.|
8005|Hamersley Group|69792|6|Mentioned|p1096 Fig.1|||||||||
8005|Hamersley Group|70086|5|Briefly described|p195-196|Paleoproterozoic|Paleoproterozoic|Geological province: Pilbara Craton. Of the Hamersley Basin.||Unit of Mount Bruce Supergroup.|Includes Boolgeda Iron Formation, Woongarra Rhyolite and Weeli Wolli Formation.|Overlain conformably by Turee Creek Group.||
8005|Hamersley Group|70509|5|Briefly described|p12-14|Paleoproterozoic|Neoarchean|Geological province: Hamersley Province; Pilbara Craton. Thickness: 2.5km.|2.63-2.45 Ga||Includes Boolgeeda Iron Formaton, Woongarra volcanics, Weeli Wolli Formation, Brockman Iron Formation, Mount McRae Shale, Wittenoom Dolomite and Marra Mamba Iron Formation.|Underlain by Fortescue Group.|Dolomite, shale and BIFs overlain by dolerite, various lava types and BIF with minor amounts of tuffs and shales.|29-JUL-19
8005|Hamersley Group|70733|6|Mentioned|p118|||Deposition rates for BIF (33-180m/m.y.) and shales and carbonate (5-12m/m.y.) applied to separate spherule layers in Marble Bar Chert Member.||||||
8005|Hamersley Group|70775|5|Briefly described|p2, p4, p13|Paleoproterozoic|Neoarchean||c. 2629-2445 Ma ||Includes the Brockman Iron Formation.|||
8005|Hamersley Group|70814|5|Briefly described|p34-p35|Paleoproterozoic|Neoarchean||2629-2445 Ma|||||
8005|Hamersley Group|70826|6|Mentioned|p8, p9|Paleoproterozoic|Neoarchean|Informally subdivided into lower and upper parts. See p6.||Mount Bruce Supergroup.||Conformably overlain by the Turee Creek Group.||13-MAY-20
8005|Hamersley Group|70936|6|Mentioned|p61|Paleoproterozoic|Archean|Geological province: Gascoyne Province, Pilbara Craton.||||||
8005|Hamersley Group|70949|6|Mentioned|p988, p998-999|Paleoproterozoic|Paleoproterozoic|||||||
8005|Hamersley Group|70958|5|Briefly described|p1, Fig. 1,  p14, 16|Paleoproterozoic|Paleoproterozoic|||||Angular unconformity with overlying Mount McGrath Formation.|Cherty banded iron formation (BIF), shale, acid igneous rocks, and dolerite sills|
8005|Hamersley Group|71003|6|Mentioned|p61|Paleoproterozoic|Archean|Pilbara Craton.||||||
8005|Hamersley Group|71042|4|Described|p64 fig 1, p65-p67||Archean|Oakover Basin.  And elsewhere in southern Pilbara. Associated with D1 deformation in this area. See also p69-p70, p72, p75-p76, p79-p80, p96, p98-p99.|ca 2700-2450 Ma|Mount Bruce Supergroup|Includes the Carawine Dolomite, Wittenoom, Mount Sylvia Formations, Mount McRae Shale, Brockman Iron Formation, Weeli Wolli Formation, Wongarra [Woongarra] Volcanics and Boolgeeda Iron Formation.|Conformably overlies the Fortescue Group.|Banded iron formations and dolomite.|28-MAY-19
8005|Hamersley Group|71112|5|Briefly described|p68-72,75,79|Neoarchean|Neoarchean|Geological province: Pilbara Craton. Deposited on a passive continental margin, showing sediment dispersal in a SW direction. Mostly exposed around the Hardey Syncline.|~2630 Ma|Unit of Mount Bruce Supergroup.||Overlain by Turee Creek Group/Kungarra Formation.||
8005|Hamersley Group|71169|5|Briefly described|p63|Siderian|Neoarchean|Hamersley Basin.|2629-2445 Ma|||||
8005|Hamersley Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||banded iron formation, dolostone, chert|
8005|Hamersley Group|71513|5|Briefly described|p66, p85, p87, p89|ca. 2450 Ma|ca. 2600 Ma|Pilbara Craton. Metamorphic temperatures peaked between 200-350 C. Origin of magnetite via decomposition Fe silicates is discussed.|||Includes the Marra Mamba Iron Formation, Wittenoom Formation, Mt Sylvia Shale, Mt McRae Shale, Brockman Iron Formation, Boolgeeda Iron Formation, Weeli Wolli Formation and the Woongara Rhyolite.|Overlies the Fortescue Group.|Banded-iron formations and ferruginous cherts.|
8005|Hamersley Group|71550|5|Briefly described|p34-36,44-45|Siderian|Siderian|Geological province: Of Hamersley Basin.|||Includes Boolgeeda Iron Formation.|Overlain by Turee Creek Group.||03-SEP-19
8005|Hamersley Group|71785|14|Not recorded|p86-91|||c. 2000 m. y.||||||
8005|Hamersley Group|71803|5|Briefly described|p366-p368|||||Mount Bruce Supergroup||||
8005|Hamersley Group|71808|4|Described|v-vi, ix, p5-p6, p8, p10, p23, p35|||Hamersley Province. 2.5km thick sequence of predominantly deep marine chemical sediments with subordinate turbiditic sediments and various intrusive and extrusive rocks. See also p42-p43, p71, p84-p85, p87, p98-p99, p101, p103, p149, p164.|ca 2630-2450 Ma|Mount Bruce Supergroup|Includes the Brockman Iron Formation, Marra Mamba Iron Formation, Mount Sylvia Formation, Weeli Wolli Formation, Woongarra Rhyolite, Boolgeeda Iron Formation, and Mount McRae Shale.|Conformably overlies the Fortescue Group. Conformably overlain by the Turee Creek Group.|Banded iron formation, hemipelagic shale, peri-platformal derived dolomite, chert, pyroclastic shale and tuff, turbiditic carbonate and turbiditic volcanics.|
8005|Hamersley Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Neoarchean|Informally subdivided into upper and lower parts. |||Includes Hamersley Group, upper; Hamersley Group, lower.|||
8005|Hamersley Group|72058|6|Mentioned|p192|Paleoproterozoic|Neoarchean|Pilbara Craton|~2630-2450 Ma.|||||
8005|Hamersley Group|72254|6|Mentioned|p360, p362, App.A p10-11|||Pilbara Craton.||Mount Bruce Supergroup|Brockman Iron Formation, Joffre Member|Underlain by Fortescue Group. Overlain by Turee Creek Group.|Includes banded iron formations (BIFs), ankeritic BIFs, shale, felsic volcanics, and dolerite.|
8005|Hamersley Group|72447|6|Mentioned|p238|||Source for Robe Formation pisoliths.|||||Includes banded iron formations.|
8005|Hamersley Group|72493|5|Briefly described|p28, 30, 33, 35|||Hamersley Basin. Deposited over c.60,000 km2. 2.5 km thick succession.|2.6 - 2.45 Ga.|Mount Bruce Supergroup.|Brockman Iron Formation.|Conformably overlies the Fortescue Group. Is overlain by the Turee Creek Group.|Dolomites, shales and BIFs in the lower part; dolerite, various lava types, BIFs and minor tuffs and shales in the upper part.|
8005|Hamersley Group|72569|5|Briefly described|p1-3|||Of the Hamersley Basin. Sedimentation of deeper strata likely occurred in quiet water below wave base and the photic zone at depths greater than 100-200m.||Mount Bruce Supergroup|Includes the Wittenoom Formation.|Conformably overlies the Fortescue Group. Overlain by the Turee Creek Group.|Shale, banded iron formation and carbonate.|
8005|Hamersley Group|72570|5|Briefly described|p2-p3|||||Mount Bruce Supergroup|Includes the Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation, Mount McRae Shale, Wittenoom Formation and the Marra Mamba Iron Formation.|Conformably overlain by the Turee Creek Group.||
8005|Hamersley Group|72705|6|Mentioned|p15-16|||Pilbara Craton. Source of some of the 2.7 -2.5 Ga zircons in the Edmund Group.||||||
8005|Hamersley Group|72712|6|Mentioned|p1, 2, 3, 4, p6-14, p9, p10 Fig.6, p50.|Paleoproterozoic|Neoarchean|See also p11 Fig.8, p31, p44. Latest source (for group constituents) Martin et al. (2000) Martin and Morris (2010).|c. 2629 +/-5 Ma to 2444 +/-3 Ma.|Mount Bruce Supergroup|Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation Mount McRae Shale, Mount Sylvia Formation, Wittenoom Dolomite/Formation, Marra Mamba Iron Formation.|Overlies Jeerinah Formation. Conformably overlies the Fortescue Group.||14-JAN-21
8005|Hamersley Group|72758|5|Briefly described|p4 Fig.1, p6, p19, p22, p23-27, p28,31|Paleoproterozoic|Paleoproterozoic|Detailed interpretations of the depositional environment of this is given by Trendall and Blockley (1970) and Trendall (1983). See also p33, p35, p55, p59.|age approx. 2.5 Ga|Mount Bruce Supergroup|Marra Mamba Iron Formation, Wittenoom Dolomite, Mount Sylvia Formation, Mount McRae Shale, Brockman Iron Formation, Weeli Wolli Formation, Woongarra Volcanics and Boolgeeda Iron Formation|Conformably overlies Fortescue Group and is conformably overlain by Turee Creek Group, or unconformably by Beasley River Quartzite, Wyloo Group.|Includes BIF with chert, podded chert, mudstone, and dolomite. Includes basalt, sandstone and other volcanics.|
8005|Hamersley Group|73022|4|Described|p1-2, p3 Fig.2, p4 Fig.3, p7 Fig.9|late Archean|late Archean|Pilbara Craton. BIF sequences deposited on a late Archean shelf, sedimentary successions suggest the presence of a land mass to the northeast. Contains chert bands between the upper Wittenoom Formation and Brockman Iron Formation forming regional marker horizons across the Hamersley province. Repeated history of fluid overpressure, micro-fracturing and hydrothermal fluid flow between 2.30 and 1.68 Ga (Rasmussen et al., 2020).|2.60-2.45 Ga|Mount Bruce Supergroup|Marra Mamba Iron Formation, Wittenoom Formation, Mount Sylvia Formation, Mount McRae Shale, Brockman Iron Formation, Weeli Wolli Formation, Woongara Rhyolite, Boolgeeda Iron Formation.|Overlies the Fortescue Group, underlies the Turee Creek Group.|Basinal shales and carbonate turbidites with mudstone, bedded chert, includes thick and laterally extensive sequences of BIF.|
8005|Hamersley Group|73102|6|Mentioned|p2 Fig.1, p4||||||Woongarra Rhyolite|||
8005|Hamersley Group|73168|6|Mentioned|p762, 765|Neoarchean|Neoarchean|Hamersley Basin. Deposited in a passive margin setting.|2630-2430 Ma||||Volcano-sedimentary sequences.|
8005|Hamersley Group|73290|5|Briefly described|p783-784|Palaeoproterozoic|Archean|Hamersley Basin. 2.5 thick succession.|||||Intercalated BIF, shale and carbonate metasediments, overlain by felsic and mafic igneous rocks.|
8005|Hamersley Group|73442|6|Mentioned|p2 Fig.1|||||||||
8005|Hamersley Group|73538|5|Briefly described|p2-8, App TbS1|||Interpreted as a sediment source for the overlying Boolgeeda Iron Formation and Turee Creek Group.||Mount Bruce Supergroup|Boolgeeda Iron Formation, Woongarra Rhyolite, Weeli Wolli Formation, Brockman Iron Formation, McRae Shale, Mount Sylvia Formation, Wittenoom Formation, Marra Mamba Iron Formation|Underlain by Jeerinah formation of the Fortescue Group. Conformably overlain by Turee Creek Group including Kungarra Formation.||
8005|Hamersley Group|73574|5|Briefly described|p762-763|Paleoproterozoic|Late Archean||||Marra Mamba Iron Formation, Wittenoom Formation|Unconformably underlies Yarraloola Conglomerate||
8005|Hamersley Group|75075|6|Mentioned|p420 Fig.1, 426|Paleoproterozoic|Neoarchean|Pilbara Craton.|c.2.4 Ga (Barley et al., 1997).|Mount Bruce Supergroup.||||
8057|Hansons Bore lamproite|41158|6|Mentioned|p160|||||||||
8075|Hardey Formation|22475|5|Briefly described|p495, Fig.3|Archean|Archean|Of the Fortescue Group. See also p498.||||||07-NOV-08
8075|Hardey Formation|22715|5|Briefly described|table7, p217|Archean|Archean|Age: 2760Ma. lower Fortescue Group.||||||13-JAN-12
8075|Hardey Formation|23045|6|Mentioned|291 fig 8|||||||||
8075|Hardey Formation|23416|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. In the Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23484|5|Briefly described|p10|Archean|Archean|Of Fortescue Group.  Age: ~2750Ma.||||||07-NOV-08
8075|Hardey Formation|23570|3|Fully described|p55|Archean|Archean|Of Fortescue Group. Age: 2768+/-16-2756+/-8Ma (U-Pb).  Overlain by the Boongal Fm.; and by Kylena Fm. in the north; underlain by Mount Roe Basalt.  Max. thickness: 3000m.  Equivalent to Cliff Springs Fm.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Boongal Formation. Geological Province Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Overlain by Kylena Formation. Underlain by Gregory Granitic Complex. Geological Province Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23585|4|Described|p15|Archean|Archean|Previously Hardey Sandstone. Of Fortescue Group. Underlain by Mount Roe Basalt. Max. thickness: 600 m.||||||07-NOV-08
8075|Hardey Formation|23594|4|Described|p13|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23598|4|Described|p13|||Previously Hardey Sandstone. Of Fortescue Group. Overlain by Kylena Formation; underlain by Mount Roe Basalt. Geological Province: Pilbara Craton.||||||16-JAN-07
8075|Hardey Formation|23612|5|Briefly described|p840|Archean|Archean|Age: ~2750 Ma. Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23745|4|Described|p10|Archean|Archean|See also page 7 Fig 5. Of Fortescue Group.||||||07-NOV-08
8075|Hardey Formation|23746|4|Described|p14|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23755|4|Described|p57|Archean|Archean|See also page 17 table 1. Of Fortescue Group.||||||07-NOV-08
8075|Hardey Formation|23780|5|Briefly described|p167|Archean|Archean|Underlain by Cheratta Granitoid Complex (unconformable).||||||07-NOV-08
8075|Hardey Formation|23783|5|Briefly described|p13 Fig.7|||Of Fortescue Group.||||||
8075|Hardey Formation|23784|5|Briefly described|p4 tb. 1|Archean|Archean|||||||07-NOV-08
8075|Hardey Formation|23789|5|Briefly described|p6 Tb. 1|Archean|Archean|Geological Province: Pilbara Craton.||||||07-NOV-08
8075|Hardey Formation|23793|5|Briefly described|p39|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin||||||07-NOV-08
8075|Hardey Formation|23794|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|23813|5|Briefly described|p112|Archean|Archean|Age: 2764Ma.  Geological Province: Pilbara Craton.||||||07-NOV-08
8075|Hardey Formation|23936|6|Mentioned|p3|||Geological Province: Hamersley Province.||||||
8075|Hardey Formation|24023|4|Described|p28|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24024|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Pilbara Craton||||||07-NOV-08
8075|Hardey Formation|24025|5|Briefly described|p13|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24184|5|Briefly described|p709|Archean|Archean|Overlan by Mount Roe Basalt. Geological Province: Pilbara Craton.||||||07-NOV-08
8075|Hardey Formation|24352|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group.   Age: ~2760Ma.   Sandstone, conglomerate, siltstone, shale and tuff.   Geological Province: Hamersley Basin||||||07-NOV-08
8075|Hardey Formation|24353|3|Fully described|p1, p9 Fig.5, p11 Tb.2|Archean|Archean|Underlain by Mount Roe Basalt (conformable). Age: 2770-2760Ma. Of the Fortescue Group. Max Thickness: 1000m. Geological Province: Hamersley Basin||||||07-NOV-08
8075|Hardey Formation|24391|4|Described|p8-4 Fig.2|Archean|Archean|Of Fortescue Group. Boulder conglomerate, sandstone (fluvial sediment). Overlies Mount Roe Basalt. Geological Province: Pilbara Block.||||||07-NOV-08
8075|Hardey Formation|24531|5|Briefly described|p36|Paleoproterozoic|Paleoarchean|Of the Fortescue Group.    Geological Province: Pilbara Craton.  See also p8-9 Fig. 3.||||||07-NOV-08
8075|Hardey Formation|24532|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group.  Thickly bedded sandstone and pebbly sandstone and cobble conglomerate.||||||07-NOV-08
8075|Hardey Formation|24533|5|Briefly described|p9|Archean|Archean|Of the Fortesque Group. Originally named Hardey Sandstone. Comprises medium to coarse-grained, poorly sorted subarkose, with locally developed conglomerate. Overlies Mount Roe Basalt. Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group.  Sandstone, conglomerate, siltstone, shale and felsic tuff.  Age: c.2760Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24541|3|Fully described|p11 Tb.2, p50|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2760 Ma. Maximum Thickness: 80m. Conformably overlies the Mount Roe Basalt and unconformably overlies rocks of the West Pilbara Granite-Greenstone Terrane. Conformably overlain by the Kylena Formation.||||||07-NOV-08
8075|Hardey Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2760Ma.  Sandstone, conglomerate, siltstone, shale and tuff.||||||07-NOV-08
8075|Hardey Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Mount Roe Basalt. Overlain by Boongal Formation. Sandstone with minor siltstone. Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|24554|5|Briefly described|p5|||Of the Fortescue Group. Conformably or disconformably overlain by the Kylena Formation at SATRIST. Geological Province: Hamersley Basin, Pilbara Craton.||||||
8075|Hardey Formation|24590|5|Briefly described|p30 Fig. 1.3|Archean|Archean|Of the Fortescue Group. Conglomerate, shale and sandstone, local tuff and agglomerate.||||||07-FEB-11
8075|Hardey Formation|42471|4|Described|p5|||Equivalent to Hardey Sandstone of Blight 1985 (86/25278).||||||
8075|Hardey Formation|42472|5|Briefly described|Map legend|Archean||||||||07-NOV-08
8075|Hardey Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
8075|Hardey Formation|42744|4|Described|p3|||||||||
8075|Hardey Formation|43119|4|Described|p6|||Of the Fortescue Group.||||||16-JAN-07
8075|Hardey Formation|43262|5|Briefly described|Map Legend||Archean|Of the Fortescue Group.||||||07-NOV-08
8075|Hardey Formation|43290|3|Fully described|p4||Archean|Of Fortescue Group.||||||07-NOV-08
8075|Hardey Formation|43698|6|Mentioned|p26|||||||||
8075|Hardey Formation|43821|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group||||||07-NOV-08
8075|Hardey Formation|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
8075|Hardey Formation|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8075|Hardey Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Sandstone, commonly feldspathic and locally tuffaceous, siltstone, shale, conglomerate, and wacke.  Age: <2756Ma.||||||07-NOV-08
8075|Hardey Formation|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8075|Hardey Formation|44837|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8075|Hardey Formation|50189|4|Described|p20-21|Archean|Archean|Of the Fortescue Group. Supersedes Hardey Sandstone. Disconformably overlies Mount Roe Basalt; unconformably overlies the Nimingarra Iron Formation. Max. Thickness: 1500m.||||||07-NOV-08
8075|Hardey Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin. Includes sandstone and siltstone; minor conglomerate.||||||07-NOV-08
8075|Hardey Formation|50300|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Geological Province: Hamersley Basin.  Age: c. 2760Ma.||||||07-NOV-08
8075|Hardey Formation|50370|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2760 Ma||||||07-NOV-08
8075|Hardey Formation|50381|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2764-2756 Ma||||||07-NOV-08
8075|Hardey Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2760 Ma||||||07-NOV-08
8075|Hardey Formation|50427|6|Mentioned|p188 Fig.9|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
8075|Hardey Formation|50544|3|Fully described|p45,p47, p15 Tb. 1|Archean|Archean|Of the Fortescue Gp.  Incl: Bamboo Cr. Member (in Oakover Sycline) and Warroo Hill and Koongaling Volcanic Members (in Gregory Range Inlier).  Disconformably overlies Mount Roe Basalt, unconformably overlies Gorge Cr. and Warrawoona Gps.  Max. thick: 1500||||||07-NOV-08
8075|Hardey Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Contains the Koongaling, Warroo Hill and Bamboo Creek Members.  Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|60112|6|Mentioned|p111 Fig.4. |||||Unit in Glen Herring Creek Sequence.||||
8075|Hardey Formation|60373|4|Described|p145 Tb. 1, p150 Tb. 2|Archean|Archean|Of Fortescue Group. Overlian by Kylena Formation, underlain by Mount Roe Basalt. Age: 2750+/-4,  2756+/-8, 2764+/-8Ma and 2768+/-16Ma (SHRIMP).||||||
8075|Hardey Formation|60429|3|Fully described|p20, Fig. 5|Archean|Archean|Superseded Hardey Sandstone. Major component of Fortescue Group on MUCCAN. Comprises 5 rock assemblages including the named Bamboo Creek Member. Disconformably overlies Mount Roe Basalt; unconformably onlaps Nimingarra iron Fm. Max. thickness: >1500m.||||||07-FEB-11
8075|Hardey Formation|60706|5|Briefly described|p625 Fig. 3, p637 Fig.9|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
8075|Hardey Formation|61259|5|Briefly described|p403|Archean|Archean|Includes the Koongaling Volcanic Member. Predominantly quartz-rich sandstone to mudstone. Overlies Mount Roe Basalt; overlain by Boongal Formation. Min. age: 2756+/-8Ma. Geological Province: Pilbara Craton.||||||07-NOV-08
8075|Hardey Formation|61265|4|Described|p43, p46-47 Fig. 2|Archean|Archean|Of the Fortescue Group. Sandstone, volcaniclastic sandstone and tuff. Age: 2775-2756 Ma (Arndt et al. 1991). Geological Province: Pilbara Craton. See also p51 Tb.2||||||07-NOV-08
8075|Hardey Formation|61266|4|Described|p58 Tb.1, p61|Archean|Archean|Of the Fortescue Group. Age: >2756 Ma (Andt et al., 1991). Conglomerate, shale and sandstone, local tuff and agglomerate. Geological Province: Pilbara Craton.||||||07-NOV-08
8075|Hardey Formation|61268|5|Briefly described|p81 Tb.1|||Of the Fortescue Group. Sandstone, mudstone, siltstone, conglomerate, felsic and mafic volcaniclastic sandstone and conglomerate and basalt flows and breccia. See also p80 Fig.2.||||||
8075|Hardey Formation|61273|5|Briefly described|p85|Archean|Archean|Contains rock used as dimension stone: Karratha Stone quarried in the Pinderi Hills.||||||07-NOV-08
8075|Hardey Formation|62129|3|Fully described|p6, p24, p25|Archaean|Archaean|Of Fortescue Gp. Disconformably overlies Mount Roe Basalt, comform overlain by Boongal Fm. Thick: 1800m.  Geol Prov: Hamersley Basin. Consists of dolerite and layered sills, siltst, mudst, conglom, volcaniclastic rock, basalt and chert.||||||24-NOV-16
8075|Hardey Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Pelite, metasandstone, metaconglomerate, metabasalt, metamorphosed volcanic sandstone, and metabasaltic breccia.||||||23-MAR-09
8075|Hardey Formation|62576|5|Briefly described|p619, p620 Fig. 3.|Archean|Archean|Of the Fortescue Group. Age:2766-2752Ma. Geological province: Pilbara Craton. Sandstone and granite boulder-pebble sedimentary conglomerate. ||||||07-NOV-08
8075|Hardey Formation|63367|4|Described|p230, p231 Fig.1|Neoarchean|Neoarchean|Deposition over a broad continental area with alluvial fan, braided fluvial, and lacustrine facies; deltaic to shoreline in the south.|2756 +/- 8 Ma (Arndt et al.,1991).|Unit in Fortescue Group.|||Variety of siliciclastic and carbonate rocks.|
8075|Hardey Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2768- 2756Ma. Overlies: Mount Roe Basalt. Sandstone, conglomerate, siltstone, shale and felsic pyroclastic rocks.||||||07-NOV-08
8075|Hardey Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup). Includes Bamboo Creek and Koongaling Volcanic Members. Age: 2772-2752Ma. Geological Province: Fortescue Basin. Sedimentary and felsic  volcanic rocks; local intrusive rocks.||||||07-NOV-08
8075|Hardey Formation|63420|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Includes the Bamboo Creek Member. Age: c.2764-2756Ma. Geol.Prov: Marble Bar Sub-basin/Hamersley Basin. Pebble to cobble conglomerate interbedded with medium- to coarse-grained sandstone, wacke and siltstone.||||||07-NOV-08
8075|Hardey Formation|63441|5|Briefly described|p38|Archean|Archean|Of the Fortescue Group. Unconformably overlies rocks of the Zebra Hill Suite. Age: c. 2760Ma. Geological province: Pilbara Craton.||||||07-FEB-11
8075|Hardey Formation|63854|5|Briefly described|p233, p234. |Neoarchean|Neoarchean|Hamersley Basin. Hosts gold placer deposits.|ca. 2765 Ma|||||
8075|Hardey Formation|64326|5|Briefly described|p71 Fig. 1, p72-73|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup). Stratigraphic detail describes Hardey Fm as it presents in the Pear Creek Centrocline (northern Hamersley Basin) - where the Fortescue Group succession is different from elsewhere.Overlies Mount Roe Basalt||||||07-FEB-11
8075|Hardey Formation|64580|4|Described|map legend|Neoarchean|Neoarchean|Of Fortescue Group. Sandstone; mudstone; siltstone; conglomerate; felsic and mafic volcanic sandstone and conglomerate; and basaltic flows and breccia; metamorphosed.||||||09-DEC-08
8075|Hardey Formation|64621|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group. Includes Bamboo Creek Member. Sandstone, siltstone, conglomerates, shale, wacke, breccia, pillow metabasalt, etc. Further details included.||||||07-NOV-08
8075|Hardey Formation|64653|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Beaton Creek and Bamboo Creek Members. Geological Province: Pilbara Craton. Sandstone, conglomerate, shale, felsic tuff, and ooidal and pisolithic beds.||||||07-FEB-11
8075|Hardey Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2766Ma - 2752Ma. Geological Province: Pilbara Craton (Hamersley Basin). Coarse to pebbly sandstone; minor pebble conglomerate; thickly bedded.||||||17-NOV-08
8075|Hardey Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Bamboo Creek Member. Geological Province: Hamersley Basin.||||||
8075|Hardey Formation|64724|4|Described|p42 Fig. 3|Neoarchean|Neoarchean|Hamersley Basin unit deposited in an intracontinental setting.||||Overlies Mount Roe Basalt.||02-APR-12
8075|Hardey Formation|64936|5|Briefly described|map legend|Archean|Archean|Of Fortescue Group, Mount Bruce Supergroup. Includes Bamboo Creek Member. Under Kylena Formation; over Mount Roe Basalt. Conglomerate sandstone siltstone shale. Age: 2764-2756 Ma (geochron: NT Arndt et al 1991). Geol. Prov: Hamersley Basin, Pilbara Craton||||||
8075|Hardey Formation|65008|4|Described|p7, p8 Fig.5, p13-15, p20-24, p29, p41 |Neoarchean|Neoarchean|Hamersley Basin. Includes 7 separately mapped facies. Defined by Thorne et al. (1991). ~1000m to less than 100m thick. Age constrained by the Bamboo Creek Member. Conglomerate contains clasts of quartz, chert, and rare mafic volcanic and granitic rocks.|2768 +/- 16 Ma -2756 +/- 8 Ma|Of the Fortescue Group|Includes Beaton Creek Member and Bamboo Creek Member.|Unconformably underlain by the Mount Roe Basalt and Corboy Formation. Conformably overlain by the Kylena Formation.|Sandstone interbedded with minor amounts of pebble to cobble conglomerate, shale and siltstone. Sandstone: feldspathic, fine to coarse grained, well-sorted or pebbly, local cross-bedding. Conglomerate: polymictic, matrix supported, upward fining.|
8075|Hardey Formation|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Includes Bamboo Creek Member. Under Kylena Fm; over Elsie Ceek Tonalite and Mount Roe Basalt. Sandstone, siltstone, conglomerate, carbonate. Age: c.2752 Ma (geochron. TS Blake etal 2004). Geol.Prov: Hamersley Basin, Pilbara Craton.||||||
8075|Hardey Formation|65726|5|Briefly described|Map legend|Archean|Archean|Hamersley Basin, Pilbara Craton. Also includes four un-named but separately-mapped sub-units.||Of Fortescue Group. |Includes Bamboo Creek Member.||Tuffaceous sandstone, siltstone and shale; accretionary lapilli and felsic tuff; feldspathic sandstone, medium- to very coarse-grained; interbedded conglomerate, wacke, sandstone and siltstone; polymictic cobble to boulder conglomerate.|
8075|Hardey Formation|65727|5|Briefly described|Map legend|Neoarchean|Neoarchean|Fortescue Basin. Also includes four un-named but separately-mapped sub-units.||Of Fortescue Group. |Includes Bamboo Creek Member.||Felsic volcaniclastic sandstone, siltstone and shale; feldspathic sandstone, pebbly sandstone and conglomerate; pebble to cobble conglomerate interbedded with sandstone, wacke and siltstone; polymictic cobble to boulder conglomerate.|
8075|Hardey Formation|65825|4|Described|p7 Fig.4,  p21, p24.|Archean|Archean|A succession of clastic sedimentary and volcanic rocks up to 3 km thick. May have been fed by the mafic plugs that intrude the Coondamar Formation.||Unit in Fortescue Group.|Includes Bamboo Creek Member.||A mixed succession: polymictic conglomerate; medium- to coarse-grained  sandstone; siltstone; local tuffaceous sandstone with accretionary lapilli; quartz-feldspar porphyry.|
8075|Hardey Formation|65827|3|Fully described|p12 Tb3, p14 Tb4, p32-36|Neoarchean|Neoarchean|Thorne et al. (1991); formerly Hardey Sandstone (MacLeod et al. 1963). Of Fortescue Group; formerly Hardey Sandstone. Includes Bamboo Creek Member. >2766 Ma - 2752 Ma SHRIMP U-Pb zircon (Blake et al. 2004). Unconformably overlies Cleaverville Formation, Mount Roe Basalt, Apex Basalt; unconformably underlies Kylena Formation; shown as equivalent to part of Nullagine Supersequence; intruded by Fortescue Group dyke. Epiclastics and volcaniclastics. 700 - 2500 m thick.||||||
8075|Hardey Formation|65828|5|Briefly described|Map legend|Archean|Archean|||Unit in Fortescue Group.|Includes Bamboo Creek Member.||Includes sandstone and siltstone, minor conglomerate.|
8075|Hardey Formation|65829|3|Fully described|p7 Fig.3, p10, pp16-17, p26, p35.|Neoarchean|Neoarchean|Formerly Hardey Sandstone (MacLeod et al. 1963); listed in the Nullagine 1:250 000 sheet (Hickman 1978); superseded, and the rocks included in the Hardey Formation (Thorne et al. 1991). Deposition of epiclastic-volcaniclastic material, thinning rapidly eastwards. Contains a high percentage of locally derived volcanic clasts, implying uplift and erosion of the Mount Roe Basalt. Costeans have been bulldozed in this unit, 1.5 km NW of Salvation Well; the mineralization searched for is not clear, although the basal part of this Formation is known to carry gold mineralization.|2766 - 2752 Ma.|Unit in Fortescue Group.|Includes Bamboo Creek Member.|Overlies unconformably the Elsie Creek Tonalite, Mount Roe Basalt and Euro Basalt.|Five units, detailed in the text: basal coarse- to fine-grained clastic sediments; felsic volcanic Bamboo Creek Member; thin-bedded clastic sediments; feldspathic clastic sediments; uppermost clastic sedimentary-volcaniclastic succession.|
8075|Hardey Formation|66108|5|Briefly described|Map legend|Neoarchean|Neoarchean|Unit in Fortescue Group. 2766-2752 Ma. Includes Bamboo Creek Member. Sedimentary and felsic volcanic rocks; local intrusive rocks.||||||
8075|Hardey Formation|66217|4|Described|p5, p6 Table 1, pp45-47, pp52-54.|Neoarchean|Neoarchean|Fortescue Basin, Pilbara Craton. Up to 3 km thick. A wide range of sedimentary and volcanic (both mafic and felsic) rocks, deposited in a continental to shallow-marine setting. Coeval with granites of Gregory Range Suite.|2764-2756 Ma.|Unit in Fortescue Group.|Includes Koongaling Volcanic Member, Bamboo Creek Member and Lyre Creek Member.|Unconformably overlies Mount Roe Basalt. Is intruded by Gregory Range Suite. Is unconformably overlain by Kylena Formation.|Basal polymict pebble conglomerate passing up into coarse-grained sandstone with pebbly sandstone and less common siltstone interbeds; local thin units of shale interbedded with siltstone and sandstone.|
8075|Hardey Formation|66685|5|Briefly described|p217-18|Archean|Archean|Diachroneity of deposition has been suggested (Hall, 2005).|2766 +/-2 Ma (zircon U-Pb, Blake et al., 2004).|Fortescue Group||Underlies the Kylena Formation, overlies the Mount Roe Basalt. Unconformably underlies the Tumbiana Formation.|Includes sandstone, shale, conglomerate, and porphyry.|
8075|Hardey Formation|67130|5|Briefly described|p3 fig 2, p12, p24 fig 17, p48|Neoarchean|Neoarchean||2766 Ma - 2752 Ma|Fortescue Group||Overlies Mount Roe Basalt, Overlain by Kylena Formation, Mount Jope Volcanics|Sandstone and felsic volcanics, ignimbrite|
8075|Hardey Formation|67183|6|Mentioned|p645 Tb.1|Archean|Archean|Present in the Southern Pilbara.||Fortescue Group||||
8075|Hardey Formation|67201|4|Described|p28-30, p49-51|||In northern Pilbara Craton, Fortescue Basin. Rapid deposition in paleovalleys of northeast Pilbara, and within shallow rift basins of northwest Pilbara. Thickness: extremely variable. Basal Fortescue Group (any of Bellary Formation, Mount Roe Basalt, Hardey Formation) unconformably overlies irregular paleosurface composed of Whundo Group, Cleaverville Formation, and Whim Creek Group.|2760-2750 Ma|Fortescue Group|Bamboo Creek Member, Cooya Pooya Dolerite, Lyre Creek Member|Unconformably overlies Mount Roe Basalt or, where absent, Whundo and Whim Creek Groups. Is unconformably overlain by Kylena Formation or Tumbiana Formation. Intruded by Cooya Pooya Dolerite.|Epiclastic deposits. Poorly sorted fluvial conglomerate and sandstone, and lacustrine shale. Polymictic conglomerate (vesicular and non-vesicular basalt derived from Mount Roe Basalt). Felsic volcanic and intrusive rocks.|24-NOV-16
8075|Hardey Formation|67202|4|Described|p51-52, p232, p236|Archean|Archean|Fortescue Basin. Thought to be coeval and comagmatic with Gregory Range Suite. Over 3km thick. Has Cu and Zn prospects in the Warroo Hill area.|2764 Ma (Arndt et al., 1991).|Fortescue Group.|Koongaling Volcanic Member, Warroo Hill Member, Tanguin Member.|Overlies Mount Roe Basalt. Is overlain by Kylena Basalt, and by the Tarcunyah Group unconformably. Faulted against Gregory Range Suite.|Rhyolite, rhyodacite, quartzite, siltstone, basalt, pelitic schist and tuffaceous volcaniclastic sandstone.|
8075|Hardey Formation|67229|6|Mentioned|p4|||NW Pilbara Sub-basin. See reference to Hardey Sandstone (p3 Fig.2).||||Is overlain unconformably by Tumbiana Formation.||
8075|Hardey Formation|67269|5|Briefly described|p5|Paleoarchean|Paleoarchean|||Fortescue Group.|||Sandstone, minor shale.|
8075|Hardey Formation|68035|5|Briefly described|p292 Fig 6, p293|Neoarchean|Neoarchean|Fortescue Basin. |2766 - 2752 Ma|Fortescue Group||Overlies Mount Roe Basalt, overlain by Kylena Formation.|Rhyolite|
8075|Hardey Formation|68056|6|Mentioned|p170-171|Archean|Archean|Pilbara Craton.||Fortescue Group.||||
8075|Hardey Formation|68101|5|Briefly described|p2, p6|Neoarchean|Neoarchean||c.2750 Ma (Blake et al., 2004).|Fortescue Group||Overlain unconformably by Kylena Formation. Overlies Mount Roe Basalt ?unconformably.|Sandstone.|
8075|Hardey Formation|68280|5|Briefly described|p5, p54|Neoarchean|Neoarchean||2766-2752 Ma|Fortescue Group||Overlain by Kylena Formation, overlies Mount Roe Basalt|Rhyolite.|
8075|Hardey Formation|68281|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin.|2766-2752 Ma (Blake et al. 2004).|Of the Fortescue Group.||Intruded by dolerite sills of the Kylena Formation .|Thickly bedded sandstone, pebbly sandstone, and conglomerate.|
8075|Hardey Formation|68282|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Ages from Arndt et al. (1991) and Blake et al. (2004). The 3 facies are mapped separately.|2766-2752 Ma |Of the Fortescue Group|||Coarse to pebbly sandstone, minor pebble conglomerate, thickly bedded; thickly bedded sandstone, pebbly sandstone and conglomerate; pebble to boulder conglomerate interbedded with medium- to coarse-grained sandstone, wacke and siltstone.|
8075|Hardey Formation|68283|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Marble Bar Sub-basin, Fortescue Basin.|c. 2764-2756 Ma (Arndt et al. 1991).|Of the Fortescue Group.|Includes Bamboo Creek Member.||Pebble to cobble conglomerate interbedded with medium- to coarse-grained sandstone, wacke, and siltstone; porphyritic dacite, rhyodacite, and rhyolite; coarse- to fine-grained alkali feldspar and quartz phenocrysts; locally as dykes.|
8075|Hardey Formation|69012|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Five unnamed sub-units are mapped separately.|2766-2752 Ma (Arndt et al 1991; Blake et al 2004)|Of the Fortescue Group.|Includes Bamboo Creek Member.||Conglomerate, sandstone, siltstone, volcaniclastic shale, wacke, rhyolite, rhyodacite and dacite, volcanic breccia, welded ignimbrite.|29-APR-14
8075|Hardey Formation|69015|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Mapped as 3 unnamed sub-units.|2766-2752 Ma (Blake et al., 2004)|Of the Fortescue Group.|||Shale and siltstone, local minor conglomerate; thickly bedded sandstone, pebbly sandstone, and conglomerate; sandstone, coarse to medium grained, generally arkosic, includes local volcaniclastic rocks.|05-MAY-14
8075|Hardey Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Includes unnamed unit of basaltic flows and volcaniclastic rock; metamorphosed.||Of Fortescue Group.|||Undivided sandstone, mudstone, siltstone and conglomerate; felsic and mafic volcanic sandstone and conglomerate; minor basaltic flows and breccia; metamorphosed.|06-MAY-14
8075|Hardey Formation|69080|5|Briefly described|p687, p693|Neoarchean|Neoarchean|||Unit in Fortescue Group.||Overlies Mount Roe Basalt. Is overlain by Boongal Formation.||
8075|Hardey Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Basaltic flows and volcaniclastic rock, sandstone, mudstone, siltstone and conglomerate. Felsic and mafic volcanic sandstone, conglomerate and breccia; metamorphosed.|
8075|Hardey Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|Includes Koongaling Volcanic Member, Tanguin Member, Warri Warri Member, Warroo Hill Member, Bamboo Creek Member, Beaton Creek Member||Porphyritic rhyolite sill; local brecciated rhyolite dykes and sanidine bearing felsic dykes. Volcaniclastic sandstone, siltstone and shale. Pebble to boulder conglomerates; thick bedded and pebbly sandstones, siltstones, shales and local wacke.|
8075|Hardey Formation|69185|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2765 Ma|Unit of Fortescue Group.||Locally intruded by Cooya Pooya Dolerite.|Undivided; sandstone; mudstone; siltstone; conglomerate; felsic and mafic volcanic sandstone and conglomerate; and basaltic flows and breccia; metamorphosed|
8075|Hardey Formation|69299|3|Fully described|p1,p5 Fig.4,p6 Tb.1,p7,p9,p12,p14-21,map|Archean|Archean|Clastic sedimentation and ultramafic to felsic volcanism. Thickness on COOYA POOYA: 0-1000 m. Extensional intracratonic sedimentary basins. Geol. Prov: Hamersley Basin, Pilbara Craton.|c. 2760 Ma, geochron, Arndt et al 1991|Of Fortescue Group.|Includes Lyre Creek Member, Coolajacka Member.|Intruded by Cooya Pooya Dolerite; correlated with Cliff Springs Formation (Hickman 1983); unconformably overlies Cherratta Granitoid Complex; disconformably or conformably overlies Mount Roe Basalt.|Lower: sandstone, conglomerate, siltstone, and shale; middle: ultramafic lava (Coolajacka Member); upper: felsic lava and volcaniclastic rocks (Lyre Creek Member).|
8075|Hardey Formation|69301|4|Described|p16-18|||Pilbara Craton. Fortescue Basin. Marble Bar Sub-basin, Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, South Pilbara Sub-basin, Sequence 2.||Fortescue Group|Bamboo Creek Member, Cooya Pooya Dolerite, Lyre Creek Member||Dominantly volcanic. Epiclastic deposits. Poorly sorted fluvial conglomerate and sandstone, and lacustrine shale in paleovalleys. Includes large volumes of felsic volcanic and intrusive rocks.|
8075|Hardey Formation|69411|6|Mentioned|p290|Neoarchean|Neoarchean|Geological province: Pilbara Craton. |||Includes Lyre Creek Member.|||
8075|Hardey Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
8075|Hardey Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Fortescue Basin. Events: Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_interpgeol_lut.csv.|2766-2749 Ma|Unit of Fortescue Group.|Includes Bamboo Creek Member, Beaton Creek Member, Koongaling Volcanic Member, Warri Warri Member, Warroo Hill  Member.||Angular boulder breccia; metabasalt and chert in sandstone matrix; sandstone; rhyolitic and volcaniclastic; siltstone, shale, conglomerate, wacke.|
8075|Hardey Formation|69792|5|Briefly described|p1096 Fig.1, p1097|Neoarchean|Neoarchean||c. 2750 Ma|. Unit in Fortescue Group.||Kylena  Formation disconformably overlies.|Fluvial sandstone.|22-JUN-20
8075|Hardey Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2766-2749 Ma|Fortescue Group|||Sedimentary and felsic volcanic rocks; local intrusive rocks.|
8075|Hardey Formation|71042|5|Briefly described|p64 fig 1, p66, p79 , p96|Archean|Archean|Oakover Basin.||Fortescue Group||||
8075|Hardey Formation|71169|5|Briefly described|p64|Neoarchean|Neoarchean||2766-2749 Ma|Fortescue Group||||
8075|Hardey Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||siltstone, greywacke, mudstone, sandstone|
8075|Hardey Formation|71803|4|Described|p366, p368, p371, p375, p380|Neoarchean|Neoarchean|Pilbara Craton. An additional age of 2752 +/- 5 Ma is derived from Blake et al, 2004.|2766 +/- 3 Ma (Blake et al, 2004)|Fortescue Group||Overlies the Mount Roe Basalt.|Terrestrial and near-shore facies clastic sedimentary rocks with lesser felsic and mafic volcaniclastic rocks and basaltic sheet flows, including minor pillow lavas.|
8075|Hardey Formation|71808|5|Briefly described|p7, p97, p104, p149|||Pilbara Craton. Deposited in a fluvial environment.||Fortescue Group|||Sandstone, siltstone, shale and conglomerate.|
8075|Hardey Formation|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.|Max age 2766+/-7 Ma, min 2749+/-5 Ma.|Fortescue Group, sequence 2||intruded by Cooya Pooya Dolerite as dykes.|Sedimentary and felsic volcanic rocks; local intrusive rocks.|
8075|Hardey Formation|72712|5|Briefly described|p8, p10 Fig.6.|Neoarchean|Neoarchean|Attains a maximum thickness of 1.8km in the Rocklea Anticline. Unconformably overlies unnamed dolerite dykes that intrude the granite greenstone terrain in the Rocklea Anticline.|c. 2763 Ma to c. 2745 Ma.|Fortescue Group|Includes Madang Tuff Member in Rocklea Anticline.|Unconformably overlies Mount Roe Basalt and granite-greenstone basement. Partially underlies Boongal and Kylena Formations. Unconformably overlies Mount Roe Basalt. Intruded by dolerite sills.|Fluvial to shallow marine sediment, conglomerate, sandstone, siltstone, mudstone, volcaniclastic rock, basalt and chert, and is intruded by up to 500 m of dolerite and layered pyroxenite sills (Thorne and Tyler, 1996).|14-JAN-21
8075|Hardey Formation|73538|6|Mentioned|p4-5, p7|Neoarchean|Neoarchean|Ages of 2752 +/- 5 Ma and 2766 +/- 3 Ma were reported by Mole et al. (2018).|2752 +/- 5 Ma, 2766 +/- 3 Ma|Fortescue Group||Underlain by Mount Roe Basalt Formation. Overlain by Kylena Formation / Boongali Formation.|Epiclastite.|
8081|Hardman Formation|7433|5|Briefly described|p25 Fig.2, p32 Fig.8, p38.|Late Permian|Late Permian|Fitzroy Sub-basin, Canning Basin. Shallow marine-deltaic clastics. Three recognisable units: lower fossiliferous shallow-marine unit; middle regressive unit with Glossopteris; upper shallow marine unit.||||Overlies Condren Sandstone.  Intercalated with/grades into Godfrey beds.||
8081|Hardman Formation|22741|5|Briefly described|p28, Table3 p12||Permian|||||||17-MAR-20
8081|Hardman Formation|22764|4|Described|Table2,p9||Late Permian|50 m. Probably conformable on Condren Sandstone; disconformable beneath Blina Shale.||||||01-FEB-10
8081|Hardman Formation|22767|5|Briefly described|Table3 p14, p22||Late Permian|||||||17-MAR-20
8081|Hardman Formation|22776|5|Briefly described|Table.3|Late Permian|Late Permian|Parent: Liveringa Group.||||||
8081|Hardman Formation|23766|5|Briefly described|p20|Permian|Permian|Parent: Liveringa Group.||||||24-NOV-08
8081|Hardman Formation|24160|4|Described|p45|Permian|Permian|||||Conformably overlies Noonkanbah Formation.|Well-bedded sandstone, fine to coarse.|
8081|Hardman Formation|29817|6|Mentioned|p12|||||||||
8081|Hardman Formation|30342|6|Mentioned|Table 20|||||||||
8081|Hardman Formation|33518|4|Described|Table 1|||||||||
8081|Hardman Formation|33519|6|Mentioned|Map legend|Permian|Permian|||||||
8081|Hardman Formation|33962|2|Defined|p50|Permian|Permian|||||||
8081|Hardman Formation|33965|6|Mentioned|p14|||||||||
8081|Hardman Formation|35120|6|Mentioned|Map legend|Late Permian|Early Permian|Early - Late PermianProb.E - L Permian||||||
8081|Hardman Formation|36020|6|Mentioned|p392|||||||||
8081|Hardman Formation|36224|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Liveringa Group.  Includes: Cherrabun, Hicks Range Sandstone and Kirkby Range Members.  Sandstone, mudstone interbedded.||||||01-FEB-05
8081|Hardman Formation|36225|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
8081|Hardman Formation|36634|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
8081|Hardman Formation|37549|6|Mentioned|Fig.12|||||||||
8081|Hardman Formation|38878|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
8081|Hardman Formation|39268|6|Mentioned|p272|||||||||
8081|Hardman Formation|40794|5|Briefly described|Fig.3|||||||||
8081|Hardman Formation|41044|6|Mentioned|p147|||||||||
8081|Hardman Formation|41071|6|Mentioned|p32|||||||||
8081|Hardman Formation|41100|6|Mentioned|p273|||||||||
8081|Hardman Formation|41158|6|Mentioned|p156|||See also p177.||||||
8081|Hardman Formation|41539|6|Mentioned|p33|||||||||
8081|Hardman Formation|41540|5|Briefly described|p21|||||||||
8081|Hardman Formation|41688|6|Mentioned|p10|||||||||
8081|Hardman Formation|41809|6|Mentioned|p65|||||||||
8081|Hardman Formation|42540|6|Mentioned|p311|||Canning Basin||||||
8081|Hardman Formation|42654|6|Mentioned|p3|||Canning Basin||||||
8081|Hardman Formation|43015|5|Briefly described|Table 1, p319|||||||||17-MAR-20
8081|Hardman Formation|43050|5|Briefly described|p12|||||||||
8081|Hardman Formation|43173|6|Mentioned|p54|Late Permian||||||||17-MAR-20
8081|Hardman Formation|43563|6|Mentioned|Fig.2,p5,Fig.9,p15||Late Permian|||||||
8081|Hardman Formation|43932|6|Mentioned|p8|||Not identified in sheet area, but Godfrey Beds may be partial equivalent.||||||
8081|Hardman Formation|44143|4|Described|p.435 Table 4-19; p.446, Figure 4-102|Permian|Permian|Unit in Liveringa Group. Up to 1000m thick; sandstone and mudstone with minor coal or limestone; shallow marine. Conformably and disconformably overlies Condren Sandstone. Type section at Mount Hardman (NOONKANBAH: 18deg 18' 45" S, 124deg 38' 52" E). Contains brachiopods, bivalves, Glossopteris and palynomorphs: Tatarian.||||||
8081|Hardman Formation|44231|5|Briefly described|Map Legend|Permian|Permian|Of the Liveringa Group. Medium-grained ferruginous sandstone; shallow marine coastal deposits. Geological Province: Canning Basin.||||||26-MAY-05
8081|Hardman Formation|45153|2|Defined|App.4-77|Tatarian|Tatarian|Originally defined as Hardman Member of Liveringa Formation.(Guppy..1958||||||19-JAN-07
8081|Hardman Formation|45158|3|Fully described|p18|||See also P36||||||
8081|Hardman Formation|46849|6|Mentioned|p188|||||||||
8081|Hardman Formation|46912|6|Mentioned|Fig.3|||Generalised stratigraphic column.||||||
8081|Hardman Formation|49644|5|Briefly described|Table|||||||||
8081|Hardman Formation|64643|6|Mentioned|p9|||Of Liveringa Group.||||||24-NOV-08
8081|Hardman Formation|64974|5|Briefly described|p148 Fig. 6, p149|Tatarian|Tatarian|Of Liveringa Group. Includes Kirkby Range and Hicks Range Sandstone and Cherrabun Member. Geological Province: Canning Basin.||||||24-JUN-09
8081|Hardman Formation|66949|4|Described|p4 Fig.2, p7, p24-25, p34, p46 Appx.2|Wuchiapingian|Wuchiapingian|See also p55 Appx.3, p60 Appx.4. Originally defined as Hardman Member (of Liveringa Formation) by Guppy et al. (1958). Divided into three Members by Yeates et al. (1975). Type section detailed. Up to 700m thick (p25 says 540m); shallow marine and fluvial deposits. Contains brachiopods, bivalves, Glossopteris and palynomorphs. Biostratigraphic zonation. Available core detailed.||Unit in Liveringa Group.|Includes Cherrabun, Hicks Range Sandstone, and Kirkby Range, Members.|Conformably and disconformably overlies Condren Sandstone.|Thinly bedded, micaceous, silty sandstone and lesser siltstone; minor coal seams and fossiliferous limestone beds.|
8081|Hardman Formation|70774|5|Briefly described|p9|Wuchiapingian|Wuchiapingian|||Of Liveringa Group.|Includes the Kirby Range Member, Hicks Range Member and the Cherrabun Member.|Overlies Lightjack Formation.||10-FEB-20
8081|Hardman Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Langfield Group.|||Fossiliferous shallow marine mottled white red-brown and dark grey micaceous sandstone, siltstone, mudstone, limestone, conglomerate; commonly ferruginised by weathering.|
8081|Hardman Formation|71623|5|Briefly described|p343, 349|||Canning Basin. Part of Dombey Cycle. Contains distinctive brachiopod faunas and Uppper Stage 5 microflora in the subsurface.|||Includes Kirkby Range, Hicks Range and Cherrabun Members.|Unconformably overlies Lightjack Formation.||
8081|Hardman Formation|72505|5|Briefly described|p890|Wuchiapingian|Wuchiapingian|Canning Basin. Correlates to the Dulhuntyispora parvithola zone.||Liveringa Group||Overlies the Lightjack Formation and the Condren Sandstone. Unconformably overlain by the Blina Shale.||
8081|Hardman Formation|73304|6|Mentioned|p71, p77|||Canning Basin. Permian-Triassic (late Changhsingian) mass extinction level occurs at the upper boundary.||||Overlain by Blina Shale.||
8091|Hargreaves Formation|13194|4|Described|p392 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: eastern Hargreaves Hills 15o20'S 128o35'E. 230-1300m thick deltaic, shallow marine deposits.||Cockatoo Group||Overlies Cecil Sandstone and Kellys Knob Sandstone (conformably). Overlain by Djilirri Limestone.|Quartz sandstone; minor dolomite and siltstone.|
8091|Hargreaves Formation|40993|6|Mentioned|p4|||||||||
8091|Hargreaves Formation|41864|3|Fully described|p54|||||||||
8091|Hargreaves Formation|41865|5|Briefly described|Map legend|Frasnian||||||||
8091|Hargreaves Formation|41867|5|Briefly described|Map legend|Frasnian||||||||
8091|Hargreaves Formation|42030|5|Briefly described|p749|||||||||
8091|Hargreaves Formation|43236|5|Briefly described|Fig.13, p13|Frasnian||Bonaparte Basin. Formerly "Cockatoo Formation".||||||
8091|Hargreaves Formation|60682|4|Described|p25 Fig. 22|Frasnian|Frasnian|Sandstone. Unconformably overlain by Buttons Formation and CEC Sandstone. Of Cockatoo Group. Geological Province: Bonaparte Basin.||||||
8091|Hargreaves Formation|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
8091|Hargreaves Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
8091|Hargreaves Formation|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
8091|Hargreaves Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
8091|Hargreaves Formation|69673|6|Mentioned|p169 fig 140|||||||||
8099|Harris Sandstone|14228|5|Briefly described|p8, p18|Tastubian|Stephanian|Condon (1954).||Lyons Group||||
8099|Harris Sandstone|23174|5|Briefly described|Fig5p8|Carboniferous||||||||
8099|Harris Sandstone|23295|6|Mentioned|p54|||Fossilized tree trunk indicates horizon is Early Permian.||||||
8099|Harris Sandstone|23726|5|Briefly described|p37|Late Carboniferous|Late Carboniferous|Of Lyons Group. Overlying unit Carrandibby Formation. Geological Province: Carnarvon Basin.||||||
8099|Harris Sandstone|23815|4|Described|p278|Carboniferous|Carboniferous|Formerly known as "Red Hill Sandstone". Geological Province: Carnarvon Basin. Underlying unit: Yindagindy Formation (disconformable). Overlying unit: Lyons Group. Contains stem fragments and trunks of Lycopodiopsis. Max. thickness: 85 m.||||||
8099|Harris Sandstone|24044|5|Briefly described|p541 Fig.2|Carboniferous|Carboniferous|||||||
8099|Harris Sandstone|24059|5|Briefly described|p146|Late Carboniferous|Late Carboniferous|Geological Province: Carnarvon Basin.||||||
8099|Harris Sandstone|32648|6|Mentioned|p32|||Westphalian.||||||
8099|Harris Sandstone|32789|3|Fully described|p82|||See also P85. Carb.-Perm. boundary.||||||15-DEC-08
8099|Harris Sandstone|33622|6|Mentioned|p89|||||||||
8099|Harris Sandstone|34085|6|Mentioned|Cor.chart|||Westphalian - Stephanian||||||
8099|Harris Sandstone|35282|6|Mentioned|Fig.2|||||||||
8099|Harris Sandstone|36257|6|Mentioned|Table 2.1|||||||||
8099|Harris Sandstone|36890|3|Fully described|p278|||Formerly Red Hill Sandstone.||||||15-DEC-08
8099|Harris Sandstone|37295|4|Described|p53|||See also Table 2.||||||
8099|Harris Sandstone|37920|6|Mentioned|p453|||||||||
8099|Harris Sandstone|40617|5|Briefly described|p13|||||||||
8099|Harris Sandstone|41271|3|Fully described|p72|||||||||
8099|Harris Sandstone|41438|6|Mentioned|Fig.11|||||||||
8099|Harris Sandstone|42116|5|Briefly described|p33|||See also Fig.12||||||
8099|Harris Sandstone|42392|5|Briefly described|p115|||||||||
8099|Harris Sandstone|42547|4|Described|p89|||||||||
8099|Harris Sandstone|43495|6|Mentioned|5|||||||||
8099|Harris Sandstone|43566|6|Mentioned|p413|||||||||
8099|Harris Sandstone|44344|14|Not recorded|p.6|||Equiv. of lowermost part of Austin Formation (G50-1).||||||
8099|Harris Sandstone|44537|14|Not recorded|map legend||Sakmarian|||||||
8099|Harris Sandstone|44657|14|Not recorded|p.5,7,8,17|||||||||
8099|Harris Sandstone|44994|5|Briefly described|p9|||U.Carb. See also P10.||||||
8099|Harris Sandstone|45015|5|Briefly described|map legend, p73|Sakmarian|Sakmarian|Quartz sandstone. Disconformably overlies Yingadindy Formation. See also p74 Fig31.||||||14-JUN-06
8099|Harris Sandstone|45016|2|Defined|p.7-12||Sakmarian|Tb, p24,27,31. (F50-13).||||||
8099|Harris Sandstone|45063|6|Mentioned|Fig. 9|||Carb.||||||
8099|Harris Sandstone|45097|6|Mentioned|Fig.|||Plants indicate L. Carb. Correlation chart.||||||
8099|Harris Sandstone|48628|14|Not recorded|p.21,25|||(F50-5/Onslow).||||||
8099|Harris Sandstone|48848|14|Not recorded|p.14|||||||||
8099|Harris Sandstone|60386|6|Mentioned|p297|Asselian|Asselian|Carnarvon Basin. Non-marine.||||||
8099|Harris Sandstone|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
8099|Harris Sandstone|64580|6|Mentioned|map legend|||Of Lyons Group.||||||15-DEC-08
8099|Harris Sandstone|64630|5|Briefly described|p31 Fig.2, p34|Gzhelian|Kasimovian|Province: Southern Carnarvon Basin. Of Lyons Group. Palynology age: D. tenuistriatus. Glacial origin, contains distinctive glacial striae.||||||24-NOV-09
8099|Harris Sandstone|67200|5|Briefly described|p7 fig 5,|Carboniferous|Carboniferous|||Lyons Group|||Crudely bedded tillite and sandstone.|
8099|Harris Sandstone|67373|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Southern Carnarvon Basin.||Unit in Lyons Group.|||Fine- to coarse-grained sandstone; minor siltstone and (near base) diamictite.|
8099|Harris Sandstone|69166|4|Described|geologyp_lut.csv|Sakmarian|Pennsylvanian|||Lyons Group|||Fine- to coarse-grained sandstone; minor siltstone and (near base) diamictite|
8099|Harris Sandstone|69297|5|Briefly described|p249|Asselian|Gzhelian|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||Lyons Group||Unconformably overlies the Quail Limestone.|Sandstones.|
8099|Harris Sandstone|70138|5|Briefly described|Map legend.|||Southern Carnarvon Basin.||Lyons Group.||Overlies Yindagindy Formation.|Fine- to coarse-grained sandstone; minor siltstone and (near base) diamictite.|
8099|Harris Sandstone|70795|4|Described|100k_geologyp_lut.csv|Sakmarian|Pennsylvanian|Also 100k_interpgeop_lut.csv|323-290 Ma||||Fine- to coarse-grained sandstone; minor siltstone and (near base) diamictite.|
8099|Harris Sandstone|71146|5|Briefly described|p6, p34|Visean|Visean|Southern Carnarvon Basin.||||Unconformably overlies the Yindagindy Formation.|Sandstone.|
8099|Harris Sandstone|72910|4|Described|p20-21, p40.|Early Permian|Late Carboniferous|Thickness mostly <50m, max 332m. Type section located northwest of Williambury Homestead, 23d48m20sS, 115d05m50sE. Includes Lepidodendroid plant fossils.Diachronous and discontinuous unit at base of Lyons Group.||Base of Lyons Group.||Overlain by the Carrandibby Formation.|Fine to coarse quartz sandstone, minor diamictite, and siltstone.|18-FEB-21
8108|Hart Dolerite|22526|6|Mentioned|Fig3 P682||Statherian|||||||
8108|Hart Dolerite|22547|3|Fully described|p23||Statherian|Age: 1790 Ma. Thickness: 3000m.||||||14-NOV-06
8108|Hart Dolerite|22716|5|Briefly described|table4, p232,236||Orosirian|Age: 1800Ma||||||
8108|Hart Dolerite|22754|5|Briefly described|p7|||Age c. 1800 Ma (SHRIMP).||||||
8108|Hart Dolerite|23125|4|Described|Table.1, p389||Proterozoic|Age: Early Proterozoic.||||||
8108|Hart Dolerite|23328|5|Briefly described|1031 Fig.3|||||||||07-SEP-09
8108|Hart Dolerite|23383|5|Briefly described|p19, p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Massive medium- to coarse-grained ophitic dolerite sill.  Intrudes the Kimberley Group as sills.  Age: c.1790Ma.  Max. thickness: 300m. Geological Province: Kimberley Basin. See also p6 Fig. 3.||||||21-JUL-15
8108|Hart Dolerite|23599|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Age: 1800 Ma.||||||07-NOV-08
8108|Hart Dolerite|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Dark grey dolerite.  Age: c.1800Ma.  Geological Province: Kimberley Basin.||||||07-NOV-08
8108|Hart Dolerite|23621|5|Briefly described|p56|||Intrudes Kimberley Group.||||||
8108|Hart Dolerite|23722|4|Described|p22|Statherian|Statherian|Age: c.1760Ma (Rb-Sr).   Intrudes the Kimberley Basin.||||||21-JUL-15
8108|Hart Dolerite|23751|4|Described|p22|Paleoproterozoic|Paleoproterozoic|Age: 1800-1790 Ma (SHRIMP U-Pb zircon).  Max. thickness: 3000 m.||||||07-NOV-08
8108|Hart Dolerite|24173|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|Age: c.1790Ma (Tyler et al, 1995)||||||07-NOV-08
8108|Hart Dolerite|24197|5|Briefly described|p132|||Continental tholeiite in the Kimberleys. Age: <1870Ma.||||||07-FEB-11
8108|Hart Dolerite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and granophyre.  Age: c.1790Ma.||||||07-NOV-08
8108|Hart Dolerite|24522|6|Mentioned|p84|Paleoproterozoic|Paleoproterozoic|Age: 1.79Ga (McElhinny and Evans 1976).  Geological Province: Kimberley Block.||||||07-NOV-08
8108|Hart Dolerite|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: c.1790Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
8108|Hart Dolerite|29380|4|Described|p10|||On Table2, Carpentarian.||||||
8108|Hart Dolerite|29845|6|Mentioned|p113|||||||||
8108|Hart Dolerite|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|30533|4|Described|p18|||On Table 13. Age 1800m.y.||||||
8108|Hart Dolerite|30636|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|30727|6|Mentioned|p45|||Palaeomagnetic pole positions||||||
8108|Hart Dolerite|30893|5|Briefly described|p205|||Lithology||||||
8108|Hart Dolerite|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|30896|4|Described|p17|||||||||
8108|Hart Dolerite|30897|6|Mentioned|p12|||Stratigraphy||||||
8108|Hart Dolerite|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8108|Hart Dolerite|31404|6|Mentioned|p257|||||||||
8108|Hart Dolerite|31446|4|Described|Table 1||Carpentarian|Unit of Kimberley Group. SD51-15,16.||||||
8108|Hart Dolerite|32108|6|Mentioned|Fig.1|||||||||
8108|Hart Dolerite|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8108|Hart Dolerite|32660|5|Briefly described|Table 3|||||||||
8108|Hart Dolerite|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
8108|Hart Dolerite|32728|6|Mentioned|Fig.3|||||||||
8108|Hart Dolerite|33443|6|Mentioned|p260|||||||||
8108|Hart Dolerite|33851|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|34137|4|Described|Table 1||Carpentarian|Carpentarian||||||
8108|Hart Dolerite|34190|4|Described|Table 2|||Proterozoic||||||
8108|Hart Dolerite|34462|4|Described|Table 1|||Carpentarian||||||
8108|Hart Dolerite|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8108|Hart Dolerite|34834|6|Mentioned|p213|||||||||
8108|Hart Dolerite|36551|4|Described|p36|||||||||
8108|Hart Dolerite|36885|4|Described|p183|||||||||
8108|Hart Dolerite|36898|6|Mentioned|p183|||||||||
8108|Hart Dolerite|37299|6|Mentioned|Fig.1|||||||||
8108|Hart Dolerite|37462|3|Fully described|p238|||||||||
8108|Hart Dolerite|37818|6|Mentioned|p78|||||||||
8108|Hart Dolerite|38071|6|Mentioned|p104|||||||||
8108|Hart Dolerite|40105|6|Mentioned|p317|||||||||
8108|Hart Dolerite|41158|6|Mentioned|p22|||||||||
8108|Hart Dolerite|41465|6|Mentioned|p12|||||||||
8108|Hart Dolerite|41594|6|Mentioned|p72|||||||||
8108|Hart Dolerite|41976|6|Mentioned|p454|||||||||
8108|Hart Dolerite|41987|5|Briefly described|Fig.4 P74|||||||||
8108|Hart Dolerite|42149|4|Described|p711|||||||||
8108|Hart Dolerite|42329|4|Described|p5|||See also Fig.2 p6||||||11-MAY-15
8108|Hart Dolerite|42710|5|Briefly described|map legend|Proterozoic||||||||
8108|Hart Dolerite|42730|6|Mentioned|p20|||||||||
8108|Hart Dolerite|42811|4|Described|p23|||||||||
8108|Hart Dolerite|42814|4|Described|p15|||age of 1800 Ma.||||||
8108|Hart Dolerite|42815|5|Briefly described|map|||||||||
8108|Hart Dolerite|42977|5|Briefly described|p275|||||||||
8108|Hart Dolerite|43281|5|Briefly described|Map legend||Proterozoic|of Kimberley Basin. Age approx 1790 Ma.||||||
8108|Hart Dolerite|43595|6|Mentioned|p75|||Emplaced at 1.76 Ga||||||
8108|Hart Dolerite|43666|6|Mentioned|p7|||||||||
8108|Hart Dolerite|43794|5|Briefly described|p319||Proterozoic|Intrusion date: 1800 Ma||||||
8108|Hart Dolerite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
8108|Hart Dolerite|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
8108|Hart Dolerite|44140|5|Briefly described|p293-294, p298-299, p304|Paleoproterozoic|Paleoproterozoic|Up to 3000 m thick. One of the world's most extensive dolerites. Coeval with Wotjulum Porphyry. Geochronology by Page (1976, after Bofinger, 1967).|1762 +/- 15 Ma (Rb-Sr).|||Intrudes Speewah and Kimberley Groups.|Tholeiitic dolerite, gabbro, granophyre; consists of several composite sills, up to 1800 m individually; up to 250 m of granophyre at the top.|07-MAR-18
8108|Hart Dolerite|44155|6|Mentioned|p253-255|Paleoproterozoic|Paleoproterozoic|Includes amphibolite from low-grade metamorphisn in King Leopold Orogen.|1760 Ma (Page et al., 1984).|||||
8108|Hart Dolerite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
8108|Hart Dolerite|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dark grey dolerite.  Age: c.1790Ma.||||||07-NOV-08
8108|Hart Dolerite|44286|5|Briefly described|Map legend|||||||||
8108|Hart Dolerite|44317|5|Briefly described|Table 2||Carpentarian|||||||
8108|Hart Dolerite|44318|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
8108|Hart Dolerite|44363|4|Described|p.13,15|||Adelaidean or Carpentarian.||||||
8108|Hart Dolerite|44364|14|Not recorded|map legend|||||||||
8108|Hart Dolerite|44366|14|Not recorded|p.12, Table 2|||Carpentarian or Adelaidean. Definition on Tech.File SE/52-5.||||||
8108|Hart Dolerite|44367|14|Not recorded|map legend|||(Reprinted 1971). Adelaidean or Carpentarian.||||||
8108|Hart Dolerite|44397|14|Not recorded|p.9,17, Table 2|||Adelaidean or Carpentarian.||||||
8108|Hart Dolerite|44398|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
8108|Hart Dolerite|44694|5|Briefly described|Map Legend||Proterozoic|||||||
8108|Hart Dolerite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
8108|Hart Dolerite|45047|5|Briefly described|p28|||See also P30. Carpentarian. 1800 my.||||||
8108|Hart Dolerite|45077|6|Mentioned|p7|||||||||
8108|Hart Dolerite|45087|5|Briefly described|p33|||Chemical analyses||||||
8108|Hart Dolerite|45140|6|Mentioned|p13|||Kimberley region.|1800 Ma.|||||
8108|Hart Dolerite|48931|3|Fully described|p57|||Silver, lead, gold, copper. See also p58. Refers Sofoulis(1968).||||||11-MAY-15
8108|Hart Dolerite|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Age: c.1790 Ma. Intrudes Speewah and Kimberley Groups.||||||07-NOV-08
8108|Hart Dolerite|50437|5|Briefly described|p5.6|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Basin.  Age: 1790 +/- 4Ma.||||||07-NOV-08
8108|Hart Dolerite|60533|5|Briefly described|p593|Paleoproterozoic|Paleoproterozoic|Age: ca 1790Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
8108|Hart Dolerite|60714|5|Briefly described|p112, p113.  |Statherian|Statherian||1790 +/- 4 Ma (U-Pb zircon: Ozchron 2004)|||Intrudes the upper units of Speewah Group and lower Kimberley Group. May be coeval with the Carson Volcanics.||
8108|Hart Dolerite|60724|5|Briefly described|p4, p5 Fig. 2|Paleoproterozoic|Paleoproterozoic|Intrudes the Speewah and Kimberley Groups. Age: 1.80Ga. ||||||07-NOV-08
8108|Hart Dolerite|61056|5|Briefly described|p785 Tb. 2|Paleoproterozoic|Paleoproterozoic|Intrudes the Kimberley Group.  Age: ca1800Ma. Time equivalent of The Granites Granite.||||||07-NOV-08
8108|Hart Dolerite|61571|5|Briefly described|p656, p657 Fig. 4|Paleoproterozoic|Paleoproterozoic|Sills and dykes intrude King Leopold Sandstone.  Age of crystallisation: 1790+/-4Ma.  Geological Province: Kimberley Basin.||||||07-NOV-08
8108|Hart Dolerite|61861|6|Mentioned|Fig.2.|||Halls Creek, eastern zone.|c.1790 Ma.|||Intrudes Kimberley Group.||
8108|Hart Dolerite|63866|5|Briefly described|p129, p133, p138|||Western Zone, Halls Creek Orogen.||||Intrudes the Kimberley and Speewah Groups.||
8108|Hart Dolerite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and granophyre.||||||12-NOV-08
8108|Hart Dolerite|64589|6|Mentioned|sample_locations file|||Sample locations.||||||12-NOV-08
8108|Hart Dolerite|64725|6|Mentioned|p57.|||North Australian Craton.|c.1830-1780 Ma.|||||
8108|Hart Dolerite|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1790 +/- 4 Ma.|||||
8108|Hart Dolerite|64748|4|Described|p268, p269 Fig 2, p270-1, 274-5, 278|Statherian||Intrudes the Speewah Group and the lower Kimberley Group; min U-Pb zircon age 1790+/-4Ma. Previous palaeomag work mentioned.||||||
8108|Hart Dolerite|66127|5|Briefly described|p147. |||Intrudes King Leopold Orogen and the Kimberley Basin; is thus found as clasts in Devonian conglomerates sourcing their sediments from these areas.|||||Fine-grained, dark-coloured.|
8108|Hart Dolerite|66526|5|Briefly described|p13, p21.|||Kimberley Province of the Hart Large Igneous Province. Mafic intrusions contain reported PGE-Au-V mineralisation.|||||Dolerite sills.|
8108|Hart Dolerite|66846|6|Mentioned|p549 Fig.2|Statherian|Orosirian|In the Western Zone of the Lamboo Complex.|||||Dolerite sills.|
8108|Hart Dolerite|67127|6|Mentioned|p107, p172|||Carbonatised and fenitised by the Yungul carbonatite dykes.|ca. 1790 Ma|||||
8108|Hart Dolerite|67354|5|Briefly described|p91.|||A granophyre boulder from this unit has been identified in core 3 near the top of the Blacktip Member of the Treachery Formation at Turtle-2; 150 km north of its outcrop, and carried by glaciation.|1,785 Ma.|||||
8108|Hart Dolerite|67563|5|Briefly described|p120, p120 Fig.1, p121, p129, p130, p131|Statherian|Statherian|SHRIMP U-Pb zircon age Page and (Sun 1994).|1790 +/- 4 Ma|||Intrudes Kimberley Group, King Leopold Sandstone, and Pentecost Sandstone.||20-JAN-17
8108|Hart Dolerite|67888|6|Mentioned|p15 fig 12, p106|Proterozoic|Proterozoic|||||||
8108|Hart Dolerite|68078|4|Described|p1, p6, p8, p9, p10, p11|Paleoproterozoic|Paleoproterozoic|Intrusion was lithologically controlled and sills showed a preference for siltstone beds in the Speewah Group. Typically forms low, rounded, boulder covered hills. Granophyre typically outcrops as cuestas and strike ridges. A younger age was derived from previous work (1762 +/- 15 Ma (Rb-Sr)) however it is now believed that the older ages given by shrimp best constrain the age of igneous crystallization.| 1790 +/- 4 Ma , 1797 +/-11 Ma (SHRIMP)|||Intrudes Speewah Group, Carson Volcanics, Warton Sandstone, Elgee Siltstone, Pentecost Sandstone|Primarily consists of tholeiitic dolerite, olivine dolerite and gabbro, and subordinate granophyre; dolerite sills and dykes. Sills up to 1800m thick.|06-SEP-22
8108|Hart Dolerite|68244|6|Mentioned|p661-662|||Kimberley Basin.||||||
8108|Hart Dolerite|68992|5|Briefly described|p498, p498 Fig.1, p503, p504, p505, p506|Statherian|Statherian||1790 +/- 4 Ma SHRIMP U-Pb (Page and Sun 1994).|||Intrudes King Leopold Sandstone, Hooper Complex, Pentecost Sandstone (locally) and Lamboo Complex. Intrudes the Kimberley Group.||
8108|Hart Dolerite|69003|5|Briefly described|p2, p5, p18-19, p21, p48 Fig.57|Paleoproterozoic|Paleoproterozoic|W zone, Lamboo Province, Halls Creek Orogen. Forms a Large Igneous Province (has an estimated minimum volume of 250 000 km3). Coeval with intrusion of San Sou Monzogranite. Also included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|c.1799-c.1795 Ma.||||Voluminous tholeiitic mafic sills and dykes; subordinate granophyre.|
8108|Hart Dolerite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|U/Pb SHRIMP age from geochron file 109639.1.pdf: 1797+/-11 Ma. Rb/Sr age: 1762+/-25 Ma|U/Pb SHRIMP cryst age: 1790+/-4 Ma||Includes unnamed granophyre|Intrudes lower Kimberley Group|Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre|21-JUL-15
8108|Hart Dolerite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv, GA_geochron.csv. |1762 Ma||||Dark grey dolerite and gabbro, pink to pale grey, medium to coarse grained granophyre.|
8108|Hart Dolerite|69585|5|Briefly described|p1, p3-5, p27, p31|Statherian|Statherian|Intrusion of about 250 000 km3. An important time marker. Possibly comagmatic with Carson Volcanics.|c.1797 Ma.|||Intrudes Speewah and Kimberley Groups.|Tholeiitic sills and dykes.|
8108|Hart Dolerite|69597|5|Briefly described|p3, p4, p6, p8 fig 4, p70 fig 57|Paleoproterozoic|Paleoproterozoic|Generated in a post-collisional magmatic event from subduction-modified mantle. Dominates the magnetic response of the Kimberley along with the Carson Volcanics. Also complicates interpretation of gravity data.  |1797 Ma|||Intrudes the Speewah and Kimberley Groups.|A network of massive dolerite sills and dykes with some granophyres.|
8108|Hart Dolerite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv and geochron files.|1790+\-4 Ma (isotopic)|||Intrudes into Carson Volcanics and Landsdowne Arkose.|Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre|
8108|Hart Dolerite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Craton. The pink to pale-grey, medium- to coarse-grained granophyre facies is un-named but mapped separately.|c.1784 Ma.||||Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|69932|6|Mentioned|p312||||1800 Ma.|||||
8108|Hart Dolerite|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|North Australian Craton. The granophyre is mapped separately.|c.1795 Ma.||||Dark-grey dolerite and gabbro, and pink to pale grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|North Australian Craton.|c.1795 Ma.|||Intrudes King Leopold Sandstone (Lower Kimberley Group).|Dark-grey dolerite and gabbro, and pink to pale grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_geologyp_lut.csv, 500k_interpgeop_lut.csv.|1791-1799 Ma||||Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|70731|5|Briefly described|p268,270,272-276,278|Statherian|Statherian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Intraplate mafic magmatism; intruded into Speewah Group and King Leopold Sandstone. Associated with the mafic Carson Volcanics, forming a LIP. Represents cessation of collisional tectonics after the end of Halls Creek Orogeny. Intruded into King Leopold Sandstone and bifurcates into 2 sill bodies within the KL Sandstone, cropping out along strike to the E on LANDSDOWNE 1:250,000 map.|c. 1797 Ma.|||||
8108|Hart Dolerite|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|North Australian Craton.|c.1795 Ma.|||Intrudes King Leopold Sandstone (Kimberley Group).|Dark grey dolerite and gabbro, and pink to pale grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|North Australian Craton.|c.1795 Ma.|||Intrudes King Leopold Sandstone (Kimberley Group).|Dark grey dolerite and gabbro, and pink to pale grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|70812|4|Described|p5-p7, p9, p11|Statherian|Statherian|Together with the Carson Volcanics is interpreted to be part of a LIP. Estimated to be c. 250 000km^3 in volume. See also p14, p18-p20, p27-p28, p30.|c. 1797 Ma|||Intrudes the Carson Volcanics.|Mafic intrusive sequence of sills of dolerite, gabbro and granophyre.|
8108|Hart Dolerite|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||Intrudes the Speewah and Kimberley Groups.||
8108|Hart Dolerite|70851|4|Described|p4-p5, p9, p11, p16|Paleoproterozoic|Paleoproterozoic|Western Zone, Lamboo Province. Rock properites and geophysical response are discussed. See also p18-p20, p24, p29-p30, p34.|c. 1797 Ma|||Intrudes the Speewah Group and the King Leopold Sandstone.|Mafic rocks, including dolerite.|
8108|Hart Dolerite|71113|5|Briefly described|p102|Statherian|Statherian|Geological province: Lamboo Province, Halls Creek Orogen. May form part of a LIP marking the end of major magmatism in the Lamboo Province. Connected Sills and dykes records part of a post-collisional magmatic event derived from subduction that modified mantle beneath the Kimberley Craton (Sheppard et al., 2012).|c. 1797 Ma|||||
8108|Hart Dolerite|71140|6|Mentioned|p102|Statherian|Statherian|With Carson Volcanics, marks the end of major magmatism in the Lamboo Province, Halls Creek Orogen.|c.1797 Ma.||||Connected sills and dykes.|
8108|Hart Dolerite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen; King Leopold Orogen. Of the Hart-Carson LIP. Event: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Hart-Carson Supersuite Magmatic Event (1797-1791 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 1m_geologyl12_lithology_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv, 1m_geologyl12_lut.csv and geochron files.|1799+\-17 to 1791+\-8 Ma (isotopic)|||Intrudes into Kimberley Group.|Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre differentiate overlies the dolerite and gabbro in some of the thicker sills|
8108|Hart Dolerite|71281|4|Described|p420-424, p429, p431|Paleoproterozoic|Paleoproterozoic|Dow and Gemuts (1967). Kimberley region. Up to 3000m thick; individual sills c.400m thick. Intrusion of these sills post-dates accretion of the Kimberley Craton onto the North Australian Craton.|1797 +/- 11 Ma (Sheppard et al., 2012).|||Intrudes Valentine Siltstone (Speewah Group) extensively, and King Leopold Sandstone and Carson Volcanics (Kimberley Group).|Gabbro, dolerite, diorite, granophyre; pyroxene granophyre differentiate overlies the dolerite and gabbro in some of the thicker sills.|
8108|Hart Dolerite|71397|6|Mentioned|p5|Statherian|Statherian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen.||||||
8108|Hart Dolerite|71784|4|Described|p84-85||Late Proterozoic|||||||
8108|Hart Dolerite|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Hart-Carson Large Igneous Province. Includes a separately mapped un-named subunit comprising pink to pale grey, medium- to coarse-grained granophyre.|1799 - 1791 Ma.|||Intrudes Speewah Group.|Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre.|06-MAY-19
8108|Hart Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen; King Leopold Orogen.|Max age 1799+/-17 Ma, min 1791+/-8 Ma.||||Dark-grey dolerite and gabbro, and pink to pale-grey, medium- to coarse-grained granophyre.|
8108|Hart Dolerite|72437|5|Briefly described|p12, p118, p123|Palaeoproterozoic|Palaeoproterozoic|Intrudes the lower parts of the Kimberley Basin succession. Descriptions can be found in Roberts et al. (1965) and Gellatly et al. (1975). Thirty nine whole rock analyses are presented in Table 19a; 29 of which are from the Dolerite and 10 from the granophyre. 13 analyses from the Speewah Valley are contained in Alvin (1993).|c. 1800 Ma||||Tholeiitic dolerite sills and less extensive granophyre.|
8108|Hart Dolerite|72490|3|Fully described|p1-6, p8, p11-13, App. A.|Statherian|Statherian|Hart-Carson Large Igneous Province, Speewah and Kimberley Basins. Emplaced within about 3 Myr. Sills have a combined thickness of about 3000 m. Represented in a feature at Speewah Dome referred to as the Speewah sill (c. 500 m thick) [also written as Speewah Sill], which was found to be an upward younging composite tabular sill [see article for detailed description] rather than a differentiated lopolithic intrusion as previously thought. Hosts vanadiferous titanomagnetite and co-genetic PGE mineralisation. Product of decompression melting of the mantle with crustal contamination and experienced closed-system fractionation from a common magma source. New magmatic ages include 1792.7 +/- 1.3 Ma, 1791.7 +/- 4.1 Ma, 1792.1 +/- 5.9 Ma.|1792.6 +/- 1.2 Ma|||Intrudes Speewah Group, including Lansdowne Arkose, and King Leopold Sandstone and lower Carson Volcanics of the Kimberley Group.|Suite of tholeiitic rocks that range from olivine-bearing gabbro to quartz-feldspar granophyre including dolerite and diorite.|
8108|Hart Dolerite|73089|6|Mentioned|p40|Statherian|Orosirian|Kimberley Basin. Similar in age to 1817-1788 Ma granitic rocks in the southern Halls Creek Orogen. Comprise part of the voluminous (300 000 km3) Hart-Carson large igneous province. Granophyre within the unit has a U-Pb zircon age of 1799 +/- 17 Ma and a U-Pb baddeleyite age of 1795 +/- 15 Ma.|[c. 1800 Ma]|||Coeval with Carson Volcanics.|Mafic sills.|
8108|Hart Dolerite|73255|6|Mentioned|p533 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
8110|Hart Spring Sandstone|13194|4|Described|p395 Tb. 4-16; p382,399 figs 4-59,-63|Middle Cambrian|Middle Cambrian|Type Section: Hart Spring 15o19'S 128o39'E. 120-300m thick tidal unfossiliferous sand flats deposits.||Unit in Carlton Group.||Overlies Tarrara Formation (conformably). Overlain by Skewthorpe Formation, and by Mulali Member (conformably). Equivalent to Eagle Hawk Sandstone (Ord Basin).|Red micaceous quartz sandstone.|
8110|Hart Spring Sandstone|14019|5|Briefly described|p24|Middle Cambrian|Middle Cambrian|Lithologically correlated with the Eagle Hawk Sandstone (Ord Basin). Geological province: Bonaparte Basin.||||||
8110|Hart Spring Sandstone|14228|5|Briefly described|p6 fig3|Cambrian|Cambrian|Southern Bonaparte Basin.||||Overlies Tarrara Formation. Overlain by Skewthorpe Formation.||05-OCT-16
8110|Hart Spring Sandstone|24390|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Geological Province: Bonaparte Basin.  Of the Carlton Group.||||||
8110|Hart Spring Sandstone|32109|6|Mentioned|Table 1|||Middle Cambrian||||||
8110|Hart Spring Sandstone|32648|6|Mentioned|p32|||M. Camb.||||||
8110|Hart Spring Sandstone|32664|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Briefly described in notes||||||
8110|Hart Spring Sandstone|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969)||||||
8110|Hart Spring Sandstone|36551|6|Mentioned|Table 16|||||||||
8110|Hart Spring Sandstone|36890|3|Fully described|p374|||||||||
8110|Hart Spring Sandstone|40993|6|Mentioned|p2|||||||||
8110|Hart Spring Sandstone|41598|6|Mentioned|p413|||||||||
8110|Hart Spring Sandstone|41840|6|Mentioned|p43|||Occurs in Bonaparte Basin||||||
8110|Hart Spring Sandstone|41864|1|Redefined|p33|||Defined 1955, redefined 1969, but type section not previously designated||||||14-MAY-14
8110|Hart Spring Sandstone|41865|5|Briefly described|Map Legend||Middle Cambrian|||||||
8110|Hart Spring Sandstone|45038|14|Not recorded|Fig 21,22,23,36||Cambrian|||||||
8110|Hart Spring Sandstone|45039|6|Mentioned|Fig.2|||Middle Cambrian.||||||
8110|Hart Spring Sandstone|45058|6|Mentioned|Fig. 3|||See also Fig. 4. Mid-Cambrian||||||
8110|Hart Spring Sandstone|48886|1|Redefined|p.37||Middle Cambrian|See also Figs, Pl.1,6,7. App,2, p.62. Middle Cambrian.||||||
8110|Hart Spring Sandstone|50085|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group.  Geological Province: Bonaparte Basin.||||||
8110|Hart Spring Sandstone|61023|5|Briefly described|p2 Fig. 2|Cambrian|Cambrian|Of the Carlton Group. Geological Province: Bonaparte Basin.||||||11-APR-08
8110|Hart Spring Sandstone|64443|6|Mentioned|p40.|||Of Bonaparte Basin. Correlative of Barkly Group, Georgina Basin.||||||
8110|Hart Spring Sandstone|64580|6|Mentioned|map legend|||Of Carlton Group.||||||15-DEC-08
8110|Hart Spring Sandstone|67860|6|Mentioned|p419 Tb. 4-18|||Of Bonaparte Basin.||||||
8110|Hart Spring Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
8110|Hart Spring Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Early Ordovician|Middle Cambrian|||Carlton Group||||
8110|Hart Spring Sandstone|69437|5|Briefly described|p22:10-11|Series 4|Series 3|Carlton Sub-basin, Bonaparte Basin, Centralian B Superbasin. Sequence 2. Peritidal to shallow-marine deposits.||Carlton Group.||Overlies Tarrara Formation. Is overlain by Skewthorpe Formation.||12-JUL-16
8110|Hart Spring Sandstone|69443|6|Mentioned|p28:21|||Bonaparte Basin.||||Correlated with Barkly Group.||12-JUL-16
8110|Hart Spring Sandstone|69448|5|Briefly described|p33:7|||Bonaparte Basin.||Carlton Group.||Correlated with Eagle Hawk Sandstone (Ord Basin).||12-JUL-16
8110|Hart Spring Sandstone|69452|5|Briefly described|p36:5|Series 4|Series 3|Carlton Sub-basin, SW Bonaparte Basin.||Carlton Group.||Conformably overlies Tarrara Formation. Is overlain conformably by Skewthorpe Formation.||12-JUL-16
8110|Hart Spring Sandstone|69673|6|Mentioned|p168 fig 139|Cambrian|Cambrian |||Carlton Group||Overlies Tarrara Formation, overlain by Skewthorpe Formation||
8110|Hart Spring Sandstone|71146|5|Briefly described|p6|Cambrian|Cambrian|Bonaparte Basin.||Carlton Group||Overlies the Tararra Formation. Overlain by the Skewthorpe Formation.|Sandstone.|
8139|Hatches Creek Group|5030|14|Not recorded|?|||From Card file.||||||
8139|Hatches Creek Group|7821|5|Briefly described|p66|||Davenport Province, Tennant Creek Inlier.|1820-1800 Ma.|||Probable correlative of the Reynolds Range Group.||
8139|Hatches Creek Group|7838|5|Briefly described|p83|||Tennant Creek Inlier.|1820-1810 Ma (U-Pb zircon: Blake and Page, 1988).|||Correlated with Reynolds Range Group.||
8139|Hatches Creek Group|22645|6|Mentioned|P212, Fig9|||||||||
8139|Hatches Creek Group|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Hanlon Subgroup, Wauchope Subgroup and Ooradidgee Subgroup.||||||07-NOV-08
8139|Hatches Creek Group|23621|5|Briefly described|p22|||Geological Province: Tennant Creek Inlier.||||||
8139|Hatches Creek Group|23733|5|Briefly described|p2, p26, p27|Paleoproterozoic|Paleoproterozoic|Includes the Wauchope Subgroup.||||||07-NOV-08
8139|Hatches Creek Group|23809|5|Briefly described|p27|||Parts correlate with the Tawallah Group (McArthur Basin).  Geological Province: Tennant Inlier.||||||30-NOV-04
8139|Hatches Creek Group|23823|5|Briefly described|p71 Fig. M1|Paleoproterozoic|Paleoproterozoic|Subdivided into Lower, Middle and Upper sections, with a total of 19 informally named formations and two members being recognised. Includes rocks previously included in the Warramunga Group. Geological Province: Davenport Geosyncline.||||||07-FEB-11
8139|Hatches Creek Group|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: ~1780Ma.  Overlies the Ooradigee Group.  Geological Province: Davenport Province (Tennant Inlier).||||||07-NOV-08
8139|Hatches Creek Group|24089|6|Mentioned|p27 Fig. 15|||||||||
8139|Hatches Creek Group|24172|4|Described|p37, p65-67 Tb.9|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek Inlier. Max. Thickness: 10,000m. Represented by Unimbra Sandstone in Tennant Creek.||||||07-NOV-08
8139|Hatches Creek Group|24173|5|Briefly described|p23|Paleoproterozoic|Paleoproterozoic|Of Davenport province (Tennant Creek Inlier). Age: c.1820Ma (Page/OZCHRON).||||||07-NOV-08
8139|Hatches Creek Group|30017|4|Described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8139|Hatches Creek Group|30320|4|Described|p422|||||||||
8139|Hatches Creek Group|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
8139|Hatches Creek Group|33102|6|Mentioned|Fig.2|||||||||
8139|Hatches Creek Group|33103|6|Mentioned|p14|||||||||
8139|Hatches Creek Group|33516|6|Mentioned|p99|||See also P101.||||||
8139|Hatches Creek Group|33699|6|Mentioned|p443|||||||||
8139|Hatches Creek Group|34053|6|Mentioned|p7|||Proterozoic||||||
8139|Hatches Creek Group|34287|6|Mentioned|p34|||||||||
8139|Hatches Creek Group|34440|6|Mentioned|p6|||L.Prot. P9||||||
8139|Hatches Creek Group|34441|6|Mentioned|p11|||L.Prot.||||||
8139|Hatches Creek Group|34810|4|Described|Table 1|||||||||
8139|Hatches Creek Group|35038|6|Mentioned|p368|||||||||
8139|Hatches Creek Group|35229|6|Mentioned|p8|||||||||
8139|Hatches Creek Group|35254|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8139|Hatches Creek Group|35771|4|Described|Table 1|||||||||
8139|Hatches Creek Group|35950|6|Mentioned|p303|||See also P308||||||
8139|Hatches Creek Group|36215|6|Mentioned|p41|||||||||
8139|Hatches Creek Group|36335|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8139|Hatches Creek Group|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8139|Hatches Creek Group|37462|5|Briefly described|p234|||See also p279.||||||25-SEP-06
8139|Hatches Creek Group|37565|6|Mentioned|Fig.5|||||||||
8139|Hatches Creek Group|37572|6|Mentioned|Fig.4|||||||||
8139|Hatches Creek Group|39566|6|Mentioned|p50|||||||||
8139|Hatches Creek Group|39571|6|Mentioned|p124|||||||||
8139|Hatches Creek Group|39621|6|Mentioned|Fig.1|||||||||
8139|Hatches Creek Group|39887|6|Mentioned|p452|||||||||
8139|Hatches Creek Group|39888|6|Mentioned|p468|||||||||
8139|Hatches Creek Group|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8139|Hatches Creek Group|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Comprises Ooradidgee, Wauchope and Hanlon Subgroups.||||||10-JAN-05
8139|Hatches Creek Group|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8139|Hatches Creek Group|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8139|Hatches Creek Group|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek Block.||||||07-NOV-08
8139|Hatches Creek Group|41129|3|Fully described|p5|||||||||
8139|Hatches Creek Group|41204|4|Described|p3|||See also p5.||||||25-SEP-06
8139|Hatches Creek Group|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||16-NOV-05
8139|Hatches Creek Group|41308|4|Described|p9|||||||||
8139|Hatches Creek Group|41310|4|Described|p6|||See also Table 1.||||||25-SEP-06
8139|Hatches Creek Group|41408|6|Mentioned|Map legend|Proterozoic||||||||
8139|Hatches Creek Group|41465|6|Mentioned|p6|||||||||
8139|Hatches Creek Group|41524|4|Described|p6|||||||||
8139|Hatches Creek Group|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Comprises the Ooradidgee, Wauchope and Hanlon Subgroups.||||||07-NOV-08
8139|Hatches Creek Group|41970|3|Fully described|p332|||||||||
8139|Hatches Creek Group|42146|6|Mentioned|p661|||||||||
8139|Hatches Creek Group|42217|5|Briefly described|p419|||||||||
8139|Hatches Creek Group|42278|6|Mentioned|p42|||||||||
8139|Hatches Creek Group|42326|5|Briefly described|p10|||||||||
8139|Hatches Creek Group|42342|5|Briefly described|p22, p23|||||||||
8139|Hatches Creek Group|42504|5|Briefly described|p61|||||||||
8139|Hatches Creek Group|42643|3|Fully described|p5, Table 1 p6-9|||Comprising 24 formations.||||||25-SEP-06
8139|Hatches Creek Group|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
8139|Hatches Creek Group|42770|5|Briefly described|Fig.14|||age of 1811 +/- 15 Ma.||||||
8139|Hatches Creek Group|42812|6|Mentioned|p60|||||||||
8139|Hatches Creek Group|42830|5|Briefly described|p169|||||||||
8139|Hatches Creek Group|42853|6|Mentioned|p593|||||||||
8139|Hatches Creek Group|42956|5|Briefly described|p31 Fig.4|||||||||
8139|Hatches Creek Group|43223|5|Briefly described|Map Legend||Proterozoic|||||||
8139|Hatches Creek Group|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8139|Hatches Creek Group|43561|6|Mentioned|p1438|||||||||
8139|Hatches Creek Group|43568|6|Mentioned|p501|||||||||
8139|Hatches Creek Group|43595|5|Briefly described|p353|||||||||
8139|Hatches Creek Group|43631|6|Mentioned|p10|||||||||
8139|Hatches Creek Group|43652|6|Mentioned|p385|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
8139|Hatches Creek Group|43697|6|Mentioned|p27|||||||||
8139|Hatches Creek Group|43749|6|Mentioned|p4|||Age (U-Pb): 1820-1800 Ma||||||
8139|Hatches Creek Group|43751|6|Mentioned|p611|||U-Pb dating: 1810-1820 Ma||||||
8139|Hatches Creek Group|43802|5|Briefly described|p77|||||||||
8139|Hatches Creek Group|44158|5|Briefly described|p38|Statherian|Orosirian|Age: ~1820-1800Ma. of Davenport Province.||||||
8139|Hatches Creek Group|44233|14|Not recorded|Fig.1||Proterozoic|||||||
8139|Hatches Creek Group|44283|14|Not recorded|p.7,10|||To N & NE of Alroy.sheet.||||||
8139|Hatches Creek Group|44285|14|Not recorded|p.6||Paleoproterozoic|Outcrops W 80 miles of Avon Downs sheet. Lower Proterozoic.||||||07-NOV-08
8139|Hatches Creek Group|44301|14|Not recorded|p.7||Paleoproterozoic|May extend onto E 53-11 from S. Lower Proterozoic.||||||07-NOV-08
8139|Hatches Creek Group|44320|14|Not recorded|p.11||Paleoproterozoic|L.Proterozoic. Table 1.||||||07-NOV-08
8139|Hatches Creek Group|44321|14|Not recorded|map legend||Proterozoic|(F53-7). Proterozoic.||||||
8139|Hatches Creek Group|44322|5|Briefly described|map legend|||?Lower Proterozoic.||||||22-DEC-09
8139|Hatches Creek Group|44944|4|Described|p.15||Neoproterozoic|Upper Proterozoic.||||||
8139|Hatches Creek Group|45032|14|Not recorded|p7||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
8139|Hatches Creek Group|45052|4|Described|p62|||L.Prot.||||||
8139|Hatches Creek Group|45140|6|Mentioned|p13|||Tennant Creek region.||||||
8139|Hatches Creek Group|45148|4|Described|p9|||Also mentioned p31.||||||25-SEP-06
8139|Hatches Creek Group|45167|3|Fully described|p14|||See also Table 1.||||||25-SEP-06
8139|Hatches Creek Group|45373|14|Not recorded|p.178|||||||||
8139|Hatches Creek Group|46830|6|Mentioned|p29|||||||||
8139|Hatches Creek Group|46842|6|Mentioned|p111|||||||||
8139|Hatches Creek Group|46844|6|Mentioned|p134|||||||||
8139|Hatches Creek Group|46864|6|Mentioned|p40|||||||||
8139|Hatches Creek Group|46868|6|Mentioned|p76|||||||||
8139|Hatches Creek Group|46919|6|Mentioned|p218|||||||||
8139|Hatches Creek Group|46991|6|Mentioned|Fig.1|||||||||
8139|Hatches Creek Group|46992|6|Mentioned|p253|||||||||
8139|Hatches Creek Group|48835|14|Not recorded|p.9, Tb.1, Pl.1|||||||||
8139|Hatches Creek Group|48844|14|Not recorded|p.13,37,66|||||||||
8139|Hatches Creek Group|48860|4|Described|p.13,15|||Tentatively correlated with Ashburton Sandstone. See base card under Ashburton Sandstone.||||||
8139|Hatches Creek Group|48891|14|Not recorded|p.8,21||Mesoproterozoic|Tb.1. Equivalent to Tawallah Group. M.Proterozoic.||||||
8139|Hatches Creek Group|48901|14|Not recorded|Not recorded||Paleoproterozoic|L.Proterozoic.||||||07-NOV-08
8139|Hatches Creek Group|48992|6|Mentioned|p63|||||||||
8139|Hatches Creek Group|48997|6|Mentioned|Fig.1|||||||||
8139|Hatches Creek Group|49033|1|Redefined|p3|Proterozoic|Proterozoic|||||||
8139|Hatches Creek Group|50353|5|Briefly described|Map Legend|||||||||
8139|Hatches Creek Group|50369|6|Mentioned|p18.2|||Of the Ooradidgee Subgroup.||||||
8139|Hatches Creek Group|50588|5|Briefly described|p2.1|||Geological Province: Tennant Creek/Davenport Province. Includes: Epenarra Volcanics.||||||
8139|Hatches Creek Group|60123|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Disconformably underlies: Hagen Member, Chabalowe Formation.||||||07-NOV-08
8139|Hatches Creek Group|60675|6|Mentioned|Map legend|||Also mentioned in relation to correlatives of the group.||||||12-JAN-05
8139|Hatches Creek Group|60681|5|Briefly described|Map legend|Statherian|Statherian|Includes the Errolola, Coulters, Yerradgi and Unimbra Sandstones, Kudinga Basalt and Newlands Volcanics.  Age: 1800-1730Ma.  Geological Province: Davenport Province.||||||11-JAN-05
8139|Hatches Creek Group|60684|4|Described|p12, p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Comprises Ooradidgee, Hanlon and Wauchope Subgroups. Sequence of clastic sedimentary, and both felsic and mafic volcanic rocks. Max. thickness: 10km. Geological Province: Davenport province.||||||14-APR-15
8139|Hatches Creek Group|60714|5|Briefly described|p121.|Statherian|Orosirian||c 1800 Ma|||Correlated with Reynolds Range Group.|Transgressive, shallow-marine, siliciclastic succession.|
8139|Hatches Creek Group|61208|6|Mentioned|p208|||||||||23-JAN-06
8139|Hatches Creek Group|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Lower and Upper Wauchope Subgroups and the Hanlon Subgroup. In the Tennant Creek region.||||||07-NOV-08
8139|Hatches Creek Group|61560|5|Briefly described|p486, p489|Paleoproterozoic|Paleoproterozoic|Folded sedimentary and volcanic rocks in the Davenport Ranges - contain both the Amelia Creek impact structure with locally abundant shatter cones, and the Kelly West structure. ||||||07-NOV-08
8139|Hatches Creek Group|61567|5|Briefly described|p631, p632, p633 Tb. 1|Paleoproterozoic|Paleoproterozoic|Comprises Ooradidgee, Wauchope and Hanlon Subgroups.  Composed primarily of well bedded sandstones in transgressive-regressive cycles, and felsic and mafic volcanic rocks.  Hosts the Amelia impact structure. Age: >1700m. Geol.Prov: Tennant Creek Inlier.||||||07-NOV-08
8139|Hatches Creek Group|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
8139|Hatches Creek Group|63866|5|Briefly described|p90, p93|||Southern Tennant Region, North Australian Craton. |c. 1815 Ma|||Unconformably overlies the Ooradidgee Group.|Shallow water sedimentary rocks and bimodal volcanics.|
8139|Hatches Creek Group|64068|4|Described|p29-31, 33, 53, 65,66, 194-197|Statherian|Orosirian|Part of basement to Georgina Basin. Age said to be Mesoproterozoic on p194. Deposited between 1860 Ma and 1760 Ma. Subsequently deformed and intruded by granites at 1820-1800 Ma and 1730-1710 Ma.|||Includes Rooneys Formation, Kurinelli Sandstone.|Unconformably overlain by Andagera Formation, Chabalowe Formation.|Felsic and less common mafic volcanics at various levels within a thick siliciclastic succession.|05-APR-12
8139|Hatches Creek Group|64722|5|Briefly described|Fig. 2 p3-6, p10, 11|Orosirian|Orosirian|Tennant region of the North Australian Craton. Age from constituent Arabulja Volcanics.|1814 +/- 4 Ma.||Includes Arabulja Volcanics.||Subaerial to shallow marine sedimentary and bimodal volcanic rocks|11-APR-12
8139|Hatches Creek Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Orosirian|Unit in the Davenport Province of the Leichhardt Superbasin. Lower part deposited during the Post-Barramundi Extension (1830-1810 Ma), upper part deposited duing the Leichhardt Extension (1800-1750 Ma)||||||
8139|Hatches Creek Group|64730|6|Mentioned|p142, Fig.11|Paleoproterozoic|Paleoproterozoic|Intruded by dolerite of age 1811 +/- 5 Ma.||||||17-SEP-14
8139|Hatches Creek Group|64735|4|Described|p205, p212 Tb1, p216, p216 Fig 15, p217|Orosirian|Orosirian|Proposed to correlate with Strzeleckie Volcanics, Tinfish Sandstone, Gwynne Sandstone, Ware Group; coeval with Ongeva Package.|1820-1800Ma.||Includes Hanlon and Wauchope Subgroups.|Overlies Ooradidgee Group.|Bimodal volcanics and siliciclastic sedimentary rocks.|20-APR-12
8139|Hatches Creek Group|64736|6|Mentioned|p221 Fig.3, p222|Orosirian|Orosirian|In Tennant Region.||||Overlies Ooradidgee Group. Unconformably overlies Warramunga Group.||30-APR-12
8139|Hatches Creek Group|64737|5|Briefly described|p232-3, p232 Fig.2, p242, p244|Orosirian|Orosirian|In Tennant Region. Coeval with Ware Group and Ongeva Package.|~1825-1800 Ma.|||Overlies Ooradidgee Group.|Sedimentary and bimodal volcanic succession.|30-APR-12
8139|Hatches Creek Group|65209|5|Briefly described|p36, p37, p38, p39|Paleoproterozoic|Paleoproterozoic|Redefined as only Wauchope and Hanlon Subgroups with layer-cake stratigraphy, overlying volcano-sedimentary succession Ooradidgee Group (former Ooradidgee and Flynn Subgroups combined). A lithostratigraphic correlation between Tomkinson Creek and Hatches Creek Groups is well founded; however, pending geochronological corroboration, the two groups have not yet been combined. Pebbles and boulders in Rising Sun Conglomerate suggest a Tomkinson Creek Group/Hatches Creek Group provenance. Units are folded concentrically or disharmonically. Geol. Prov: Davenport Province.|||Wauchope Subgroup, Hanlon Subgroup.|Overlies Warramunga Group unconformably (angular unconformity) and Ooradidgee Group.||05-JAN-17
8139|Hatches Creek Group|65222|5|Briefly described|p111, 125, 126|||Felsic volcanism at and near base. Volcanics part of Group are ~1829-1880 Ma by conventional U-Pb dating. |||Includes Treasure Volcanics, Epenarra Volcanics|Unconformably overlies Warramunga Formation in the south. Lower part may correlate with Flynn Subgroup.||
8139|Hatches Creek Group|65232|5|Briefly described|p78|||With Tomkinson Creek Group, are correlatives of Katherine River Group and Tolmer Group. Affected by deformation and granite intrusion. Lower part contains fluvial sandstone  interbedded with locally thick volcanic units. Geol Prov: Tennant Province.||||||09-FEB-10
8139|Hatches Creek Group|65333|5|Briefly described|Map Legend|Statherian|Statherian|Includes Errolola Sandstone (Hanlon Subgroup) and Kudinga Basalt, Coulters Sandstone, Newlands Volcanics, Unimbra Sandstone (Wauchope Subgroup). Of Davenport Province, Tennant Region, NT.||||||
8139|Hatches Creek Group|65334|5|Briefly described|Map Legend|Statherian|Statherian|Includes Hanlon Subgroup and and Wauchope Subgroup. Of Davenport Province, Tennant Region, NT.||||||
8139|Hatches Creek Group|65336|6|Mentioned|Map Legend|||shown only in section||||||
8139|Hatches Creek Group|65338|3|Fully described|p iv, p6, pp19-20.|Paleoproterozoic|Paleoproterozoic|Tennant Region. Lithostratigraphic correlative of Tomkinson Creek Group. Probably correlates with Reynolds Range Group. Predominantly fluviatile and shallow-marine or intertidal sedimentation and subaerial felsic volcanic rocks.|c.1810 - 1790? Ma.||Includes Wauchope and Hanlon Subgroups. Includes Unimbra, Coulters and Erololla Sandstones.||Predominantly a layer-cake succession of ridge-forming quartz-rich sandstones, recessive feldspathic and lithic sandstones, volcanic rocks, siltstone and minor calcareous rocks.|
8139|Hatches Creek Group|65342|5|Briefly described|p13. |Paleoproterozoic|Paleoproterozoic|Outcrops extensively in the Tennant Region. Is subsurface in the Wiso Basin (Lander Trough). Several thousand metres thick.|||||Predominantly volcanosedimentary succession of sandstone, felsic and mafic volcanic rocks, subordinate siltstone and conglomerate; minor carbonate rocks.|
8139|Hatches Creek Group|65358|4|Described|p13, p16|Paleoproterozoic|Paleoproterozoic|In SE of Arunta Region. Includes Ooradidgee, Wauchope and Hanlon Subgroups. Well-exposed. Makes up most of Davenport Province. >10 km thick succession of sandstone and bimodal volcanics with minor carbonate rocks. Deposited in an intracratonic basin.||||||
8139|Hatches Creek Group|66767|5|Briefly described|p57|||Davenport Province, Tennant Region.|||Wauchope, Hanlon Subgroups.|Overlies Ooradidgee Group, locally conformably to unconformably. Correlated with Reynolds Range Group.|A succession of shallow-marine and fluviatile sandstone, and predominantly subaerial felsic volcanic rocks including lava and ignimbrite.|
8139|Hatches Creek Group|67148|5|Briefly described|Map legend.|Orosirian|Orosirian||||Includes Wauchope and Hanlon Subgroups.|Overlies Ooradidgee Group.||
8139|Hatches Creek Group|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Unimbra Sandstone and Newlands Volcanics.|||
8139|Hatches Creek Group|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Not shown on legend because it does not outcrop in map area.|||Includes Newlands Volcanics, Coulters Sandstone and Kudinga Basalt.|||
8139|Hatches Creek Group|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Wauchope and Hanlon Subgroups.|||
8139|Hatches Creek Group|67227|14|Not recorded|?|||||||||
8139|Hatches Creek Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area.|~1820-1800 Ma.||Yaddanilla, Canulgerra, Alinjabon, Errolola, Coulters, Yeeradgi, Unimbra Sandstones; Vaddingilla, Lennee Creek Formations; Kudinga Basalt; Arabulja, Treasure Volcanics.|Time-equivalent to lower Tomkinson Creek Group. Overlies Ooradidgee Group.||
8139|Hatches Creek Group|67352|4|Described|v, p3, p8, p9, p50, p57, p59|Statherian|Orosirian|Mostly siliciclastic but with volcanics in the Wauchope Subgroup. Copper minerals in basalts. Uranium anomalies in acid rocks. Forms high bevelled ridges and uplands. Thickness c.10,000 m.|||Wauchope and Hanlon Subgroups.|Intruded by Devils Suite. Overlies Ooradidgee Group.||
8139|Hatches Creek Group|68518|3|Fully described|p5, p6-10 Tb. 1, p11, p13|Proterozoic|Proterozoic|Of Sullivan (1953) and Hossfield (1954), and slightly modified by Smith and others (1961) and Ryan (1961). Joint venture (BMR and NTGS in 1981-83) resulted in 3 subgroups and 21 formations and 2 members (Blake and others, 1985). All, but 4 formations and 1 member, crop out in Elkedra region. Characterised by ridge-forming arenites separated by less-resistant sedimentary and volcanic rocks. Thickness: probably at least 10 000 m. Correlates with Tomkinson Creek beds. Age: postdates tight folding (1810 Ma) of Warramunga Group, and before intrusion of Elkedra Granite (1640 Ma). This unit was folded and displaced by faults before Elkedra Granite was emplaced in SE. Regional metamorphism to mainly greeschist facies.|between 1810 Ma and 1640 Ma||Ooradidgee Subgroup, Wauchope Subgroup and Hanlon Subgroup|Unconformably overlies Warramunga Group (north of Elkedra region). Intrusion by Elkedra Granite postdates folding. Unconformably overlain by Andagera Formation and Sandover beds.|Sequence of shallow-marine to fluvial sedimentary rocks and interlayered felsic and mafic volcanics.|
8139|Hatches Creek Group|68697|5|Briefly described|p24, p46||||||Unimbra Sandstone, Arabulja Volcanics, Yeeradgi Sandstone.|Conformably and transitionally overlies Ooradidgee Group.||
8139|Hatches Creek Group|69187|4|Described|p52, p54 Fig.3, p55|Paleoproterozoic|Paleoproterozoic|Hatches Creek Province. Lower part of Hatches Creek Group is distinguished from Tomkinson Creek Group by presence of felsic and mafic volcanic units. Contains felsic volcanic unit with age of 1814 +/- 3 Ma.||||overlies Ooradidgee Group|shallow marine sedimentary rocks; contains felsic porphyries|
8139|Hatches Creek Group|69417|5|Briefly described|p2:5-6|Orosirian|Orosirian|Davenport Province.|c.1810-1770 Ma.|||Is intruded by Treasure Suite. Correlated with Tomkinson Creek Group.||12-JUL-16
8139|Hatches Creek Group|69424|5|Briefly described|p9:2, 4-5, 8, 10, 26-28, 32, 34, 54|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Davenport Province. There is one local minor outcrop in the Warramunga Province. Previously (Blake et al., 1985) included rocks now assigned to the Ooradidgee Group. Deformation during the Davenport Event is described.|||Wauchope, Hanlon Subgroups; Newlands, Arabulja and Strzeleckie Volcanics; Rising Sun Conglomerate?.|Overlies Ooradidgee Group unconformably or conformably. Correlated with Tomkinson Creek Group.||12-JUL-16
8139|Hatches Creek Group|69425|4|Described|p10:1-4, 10-20, 22-25|Statherian|Statherian|Redefined by Blake et al. (1985) to include the Ooradidgee, Wauchope and Hanlon Subgroups. Subsequently Donnellan et al. (2001) combined the Ooradidgee and Flynn Subgroups and excluded them from this Group to form their own (Ooradidgee) Group. The extent of this unit defines the Davenport Province, southern Tennant Region. 19,500 km2 exposed in Murchison and Davenport Ranges; and 2,000 km2 in Osborne and Crawford Ranges as an outlier on the margins of Aileron Province. Extends under cover below Wiso and Georgina Basins. Deformation (which is described in some detail) by the Davenport Event was thought to predate the Elkedra Granite, which cuts across folds in Rooneys Formation. Metamorphosed mostly to greenschist facies. Proposed part-correlation with the Reynolds Range Group has been questioned by Claoue-Long, who suggests alternative correlations with Mount Charles Formation, Gardiner Sandstone, Birrindudu or Limbunya Groups are possible on geochronological grounds.|||Wauchope and Hanlon Subgroups; Unimbra Sandstone.|Is overlain unconformably by Andagera Formation. Correlated with Tomkinson Creek Group and ?Strangways Metamorphic Complex.||12-JUL-16
8139|Hatches Creek Group|69426|6|Mentioned|p11:7|||Davenport Province (Tennant Region).||||||12-JUL-16
8139|Hatches Creek Group|69427|6|Mentioned|p12:3, 8, 13|||Aileron Province.|||Wauchope Subgroup.|||12-JUL-16
8139|Hatches Creek Group|69429|6|Mentioned|p14:3|||See Donnellan et al. (2001). Davenport Province and South Lake Woods inliers. Probable correlates, consisting of quartz sandstone and minor siltstone, chert and quartzite, crop out in SOUTH LAKE WOODS and WINNECKE CREEK  map areas. They are probably surface expressions of basement for the Wiso Basin.||||||12-JUL-16
8139|Hatches Creek Group|69431|5|Briefly described|p16:1-2, 5, 8, 22|||Davenport Province. Possibly correlated with Ongeva Package, Reynolds Range Group, Ledan Schist, Utopia Quartzite, Mendip Metamorphics, Mount Charles Formation and Pargee Sandstone. Folding during the Davenport Event is discussed.|||Wauchope, Hanlon Subgroups.|Correlated with Tomkinson Creek Group.||12-JUL-16
8139|Hatches Creek Group|69443|5|Briefly described|p28:12, 18|Paleoproterozoic|Paleoproterozoic|A major source of sediments for the overlying Andagera Formation.||||Is overlain unconformably by Andagera and Chabalowe Formations.||12-JUL-16
8139|Hatches Creek Group|69447|5|Briefly described|p32:1|Proterozoic|Proterozoic|Tennant Region. Forms part of the basement for the Wiso Basin.||||||12-JUL-16
8139|Hatches Creek Group|69673|6|Mentioned|p3 fig 2, p17, p142|Orosirian|Statherian|||||Correlated with Groote Eylandt Group||
8139|Hatches Creek Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Province. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Tawallah Group (central/southern McArthur Basin) and Birrindudu and Tolmer groups (Birrindudu Basin).||||||
8139|Hatches Creek Group|72379|5|Briefly described|p7|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Intruded by mineralised quartz veins. At the Pioneer deposit (Hatches Creek tungsten field), the veins present as en-echelon, south dipping mineralised quartz veins of <1 m width extend for 90-165 m, striking ENE. Sample FR18MVM001 is from a molybdenite-scheelite-wolframite-bearing quartz vein from the Pioneer deposit. ID-NTIMS analysis of molybdenite from Sample FR18MVM001 yielded a model age of 1714+\-8 Ma, broadly consistent with previous Ar-Ar results, and support the interpretation of a direct mineralisation age for this deposit; it suggests a broadly consistent mineralising episode across the Hatches Creek tungsten field at ca 1720-1680 Ma.|||||Sandstone, greywacke, some quartzite, siltstone.|
8139|Hatches Creek Group|72380|5|Briefly described|p1,6|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.|||||Interbedded siltstone, sandstone, quartzite and volcanic rocks; acid porphyry.|
8139|Hatches Creek Group|72711|6|Mentioned|p2.|Orosirian|Orosirian|Davenport Province.|> 1810 Ma.||Gwynne Sandstone?||Includes siltstone, sandstone, volcanic and metasedimentary assemblages.|
8139|Hatches Creek Group|72718|6|Mentioned|p12|||||||||
8139|Hatches Creek Group|73083|6|Mentioned|p9, p20, p41|||Davenport Province. Deposited between ca 1820-1805 Ma (Donnellan, 2013). Not equivalent to Ledan Schist.|1820-1805 Ma||Wauchope Subgroup, Coulter Sandstone, Kudinga Basalt|||
8139|Hatches Creek Group|73128|5|Briefly described|p13|||Present as surface outcrop at Prospect D, Taylor 1:100 000 map sheet. Cross-cut by a km-length dyke of metagabbro that host / is associated with mineralisation.|||Strzeleckie Volcanics|Unconformably underlain by Warramunga Formation. Intruded by Elkedra Granite.|Includes sedimentary and metasedimentary rocks.|
8139|Hatches Creek Group|73550|6|Mentioned|p5|||||||||
8139|Hatches Creek Group|73590|6|Mentioned|p1|||||||||
8205|Headleys Limestone|14019|3|Fully described|p21|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Overlies the Antrim Plateau Volcanics.  Copper mineralisation at the contact.  Geological Province: Ord Basin.||||||
8205|Headleys Limestone|22537|5|Briefly described|40|||||||||
8205|Headleys Limestone|22547|4|Described|p30||Early Cambrian|Of the Negri Subgroup. Geological province: Ord Basin. Thickness: 50 m. Overlies Antrim Plateau Volcanics. Overlain by Ranford Formation.||||||14-NOV-06
8205|Headleys Limestone|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
8205|Headleys Limestone|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|Of Negri Subgroup. Geological Province: Ord Basin. Max. thickness: 20 m.||||||
8205|Headleys Limestone|23821|4|Described|p244|Middle Cambrian|Middle Cambrian|Of Negri Group. Geological Province: Ord Basin.||||||
8205|Headleys Limestone|28255|3|Fully described|p94-95, p82|Middle Cambrian|Middle Cambrian|Basal unit of the Negri Group. Massive limestone. Disconformably overlies Antrim Plateau Volcanics; conformably underlies Nelson Shale. Max. thickness: 40m. Geological Province: Hardman and Rosewood Basins (extensive outcrops). See also Tb. 9 (before p83)||||||
8205|Headleys Limestone|30895|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
8205|Headleys Limestone|32172|4|Described|Table 2|||Middle Cambrian||||||
8205|Headleys Limestone|32173|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Group.  Grey crystalline limestone.||||||16-NOV-04
8205|Headleys Limestone|32469|6|Mentioned|p533|||||||||
8205|Headleys Limestone|32648|6|Mentioned|p32|||L. Camb.||||||
8205|Headleys Limestone|33375|6|Mentioned|p3, p14|||Of Hardman (1885) who gave the unit an age of Carboniferous. Basal unit of Negri Group.||||||27-APR-05
8205|Headleys Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
8205|Headleys Limestone|33378|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Grey, massive, finely crystalline limestone.||||||27-APR-05
8205|Headleys Limestone|33443|6|Mentioned|p260|||||||||
8205|Headleys Limestone|36551|6|Mentioned|p22|||See also Table 16.||||||
8205|Headleys Limestone|36890|3|Fully described|p396|||||||||
8205|Headleys Limestone|39210|5|Briefly described|Fig.18|||||||||
8205|Headleys Limestone|40993|6|Mentioned|Fig.1|||||||||
8205|Headleys Limestone|41840|1|Redefined|p41|Middle Cambrian|Early Cambrian|Age: Early to early Middle Cambrian||||||
8205|Headleys Limestone|41864|4|Described|p18|||||||||
8205|Headleys Limestone|41865|6|Mentioned|Map Legend|Middle Cambrian||||||||
8205|Headleys Limestone|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
8205|Headleys Limestone|42771|6|Mentioned|p14|||||||||
8205|Headleys Limestone|43299|5|Briefly described|Map Legend||Cambrian|of Negri Subgroup.||||||
8205|Headleys Limestone|43606|6|Mentioned|p5|||||||||
8205|Headleys Limestone|43853|5|Briefly described|Map Legend||Ordian|||||||
8205|Headleys Limestone|43855|5|Briefly described|Map Legend||Ordian|||||||
8205|Headleys Limestone|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
8205|Headleys Limestone|44317|4|Described|Table 4||Cambrian|||||||
8205|Headleys Limestone|44318|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
8205|Headleys Limestone|44324|14|Not recorded|p.11||Cambrian|Tb.3. (Cambrian).||||||
8205|Headleys Limestone|44325|14|Not recorded|map legend||Middle Cambrian|M.Camb.||||||
8205|Headleys Limestone|44363|5|Briefly described|p.6,18,20,27||Middle Cambrian|Middle Cambrian (Negri Group).||||||
8205|Headleys Limestone|44364|14|Not recorded|map legend|||||||||
8205|Headleys Limestone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
8205|Headleys Limestone|44965|14|Not recorded|Not recorded|||||||||
8205|Headleys Limestone|45047|6|Mentioned|p104|||||||||
8205|Headleys Limestone|48943|3|Fully described|p107|||Stratigraphy.||||||
8205|Headleys Limestone|48950|6|Mentioned|p41|||||||||
8205|Headleys Limestone|60419|3|Fully described|p1, 3 Fig.2, p5|Middle Cambrian|Middle Cambrian|Of Negri Subgroup. Conformably overlies Antrim Plateau Volcanics. Conformably overlain by Nelson Shale. Max. thickness: 40 m. Microbial laminate, stromatolites. Intertidal to supratidal depositional environment. Geological Province: Ord Basin.||||||10-FEB-05
8205|Headleys Limestone|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group). Grey massive to laminated limestone; contains minor chert and stromatolites locally. Geological Province: Ord Basin.||||||03-NOV-04
8205|Headleys Limestone|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Negri Subgroup (Goose Hole Group).  Grey stromatolitic limestone, minor chert.  Unconformably overlies the Antrim Plateau Volcanics; conformably overlain by Nelson Shale. Geological Province: Ord Basin.||||||24-NOV-04
8205|Headleys Limestone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
8205|Headleys Limestone|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Ord Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
8205|Headleys Limestone|65417|5|Briefly described|p165.|Cambrian|Cambrian|Locally overturned on the western limb of the Hardman Syncline, due to post-Frasnian transpression.||||||
8205|Headleys Limestone|67151|5|Briefly described|Map legend.|Cambrian|Cambrian|Ord Basin.||Unit in Goose Hole Group.|||Grey, massive, finely crystalline limestone.|
8205|Headleys Limestone|67860|4|Described|p417,421 Figs.4-85,86; p420 Tb.4-18|Middle Cambrian|Middle Cambrian|35-50 m thick. Type section details given. Contains stromatolites.||Negri Subgroup||Conformably overlies Antrim Plateau Volcanics. Overlain conformably by Nelson Shale.|Grey micritic limestone with chert nodules; minor siltstone.|
8205|Headleys Limestone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Series 3|Series 3|Ord Basin||Negri Subgroup|||grey micritic limestone with chert nodules; minor siltstone|
8205|Headleys Limestone|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 500k_geologyp08_lut.csv. ||Negri Subgroup|||Grey micritic limestone with chert nodules; minor siltstone.|
8205|Headleys Limestone|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Ord Basin, Centralian B Superbasin. Sequence 1.||Negri Subgroup.||Is overlain by Nelson Shale.||12-JUL-16
8205|Headleys Limestone|69445|5|Briefly described|p30:5, 10-11, 16-17|Middle Cambrian|Middle Cambrian|Mory and Beere (1988). Ord Basin. Associated with widespread but economically insignificant Cu mineralisation, near and along the contact with Antrim Plateau Volcanics.||||Unconformably overlies Antrim Plateau Volcanics.||12-JUL-16
8205|Headleys Limestone|69448|4|Described|p33:1-5, 8-9|Middle Cambrian|Middle Cambrian|Traves (1955). Ord Basin. Small outliers occur in western WATERLOO map area. 35-50m thick. Intertidal to possibly supratidal environment of deposition. Forms bold karstified exposures, from cuestas to parallel-sided walls up to 50m high. Ordian age. Brittly deformed by the long-lived Negri Fault which is also associated with copper mineralisation. Is also offset by the Limbunya Fault.||Negri Subgroup.||Disconformably overlies Antrim Plateau Volcanics. Is overlain conformably by Nelson Shale.|Medium- to thickly-bedded microbial laminite with stromatolites, basal beds with ovoid and flat siliceous nodules; overlain by slightly wavy, thinly-bedded limestone and small siliceous spheroidal nodules, ripple marks.|12-JUL-16
8205|Headleys Limestone|69634|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|505-497 Ma (Inferred)|Unit of Negri Subgroup.|||Grey micritic limestone with chert nodules; minor siltstone|
8205|Headleys Limestone|69673|5|Briefly described|p192, p193, p194|Cambrian|Cambrian |35-50m thick.||Negri Subgroup||Overlain by Nelson Shale|Microbial laminite and bedded limestone,|
8205|Headleys Limestone|70154|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian||497-505 Ma|Negri Subgroup|||Grey micritic limestone with chert nodules; minor siltstone.|
8205|Headleys Limestone|70655|5|Briefly described|Map Legend|Cambrian|Cambrian|Ord Basin.||Goose Hole Group.|||Grey, massive, finely crystalline limestone.|
8205|Headleys Limestone|71267|4|Described|GEOL_LUT_CSV files|Series 3|Series 3|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|505-497 Ma (inferred)|Unit of Negri Subgroup.|||Grey massive to laminated limestone; minor chert and stromatolites|
8205|Headleys Limestone|71800|5|Briefly described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin.||Negri Subgroup||Overlain by the Nelson Shale.||
8205|Headleys Limestone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Antrim Plateau Basalt, underlies the Nelson Shale.||
8223|Heavitree Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Amadeus Basin||||||
8223|Heavitree Formation|23983|5|Briefly described|p19|||||||||
8223|Heavitree Formation|34186|6|Mentioned|Fig.3|||Late Precambrian. See also Fig.4.||||||
8223|Heavitree Formation|67128|5|Briefly described|p30, p33|||Considered to be the base of the (northeastern) Amadeus Basin. Also appears as Heavitree Quartzite on p33. Has distinctly different provenance from MacDougall Formation.|c.1198 Ma (maximum depositional age).|||||
8223|Heavitree Formation|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Murraba Basin, Centralian Superbasin.||||Is overlain by Bitter Springs Group.|Quartz sandstone and quartzite; lesser siltstone and pebbly conglomerate.|
8223|Heavitree Formation|71080|5|Briefly described|p4, p9, 23, 26, 29, 30|Tonian|Tonian|Amadeus Basin. Maximum age constrained by underlying unit. Supersequence 1. Part of Gillen-Heavitree pertroleum system. Provides sandstone reservoir for source rocks in overlying Gillen Formation.|< 976 +/- 3 Ma.|||Unconformably underlain by Central Desert Dolerite Suite. Overlain by Gillen Formation. Correlated with Munyu Sandstone, Dean Quartzite, Kulail Sandstone; Vaughan Springs Quartzite.|Dominantly sandstone.|
8223|Heavitree Formation|71344|5|Briefly described|p1093, 1094|||Basal unit of Amadeus Basin. Fluvio-deltaic depositional environment. Natural gas in Magee 1 contains 6% helium.||||Discordantly overlies metamorphic basement of Arunta region.||
8223|Heavitree Formation|71801|6|Mentioned|p231|Neoproterozoic|Neoproterozoic|Amadeus Basin.|ca. <1000 Ma |||||
8223|Heavitree Formation|71810|5|Briefly described|Map legend.|Tonian|Tonian|Amadeus Basin (Phase 1), Centralian Superbasin.|<975 Ma.|||Overlies Tjauwata Group. Is overlain by Bitter Springs Group.|Quartz sandstone and quartzite; lesser siltstone and pebbly conglomerate.|
8223|Heavitree Formation|71841|5|Briefly described|p1-2|Cryogenian|Cryogenian|Of Amadeus Basin.||||Equivalent to Dean Quartzite. Overlain by Gillen Formation. Underlain by basement.||
8223|Heavitree Formation|71842|6|Mentioned|p1, p3|Cryogenian|Cryogenian|Of Amadeus Basin. See Heavitree Quartzite.||||||08-JAN-20
8223|Heavitree Formation|72034|6|Mentioned|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Informal grouping of units convenient to map scale.||||||
8223|Heavitree Formation|72259|6|Mentioned|p10|||||||||
8223|Heavitree Formation|72375|4|Described|p1-2,5-9,11,25|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Type area: Limbla Cliffs, southeastern LIMBLA 1:100 000 map sheet. Formerly known as Heavitree Quartzite (of Joklik 1955). Basal stratigraphic unit of the Amadeus Basin. Only exposed along the present day northern margin of the basin. Structurally interleaved with Aileron Province basement rocks; isoclinally infolded with Atneequa Suite (Kositcin et al 2011, Whelan et al 2011) and Moonlight gneiss (Whelan et al in prep) on LIMBLA and ILLOGWA CREEK mapsheets. Previous detrital zircon studies yielded maximum depositional ages between 1050-1000 Ma, and zircon provenance studies have identified the Musgrave Province and Arunta region as dominant sediment sources (see p5 for references). SHRIMP U-Pb zircon analysis by Kositcin et al., 2014 yielded an interpreted max depositional age (206Pb/207Pb) of 1050+\-21 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS IC13CJE002 (silicified coarse-grained sandstone) and NTGS IC12JAW1801 (quartzite) suggest they crystallised in magmas derived from a range of crustal sources (see p6 and p8 for Hf isotopic results and interpretations for NTGS IC13CJE002 and NTGS IC12JAW1801 respectively).|1073 +/- 12 (max dep age)|||Overlain paraconformably by Gillen Formation. Correlable with Dean Quartzite. Equivalent to Vaughan Springs Quartzite, Yackah beds, Stanovos Quartzite.|Silicified, well-bedded, fine- to medium-grained quartz sandstone with common sedimentary structures such as ripple marks and cross-beds. Quartzite is also present.|04-DEC-19
8223|Heavitree Formation|72489|6|Mentioned|p4 Fig.3|Tonian|Tonian|Amadeus Basin, including the Limbla Syncline. Only shown on p4 Fig.3. Simplified geological maps.||||Underlies the Bitter Springs Group.||14-SEP-20
8223|Heavitree Formation|72516|6|Mentioned|p85-86|Tonian|Stenian|Amadeus Basin. Formerly the Heavitree Quartzite. Age is also derived from Maidment 2005, Maidment et al, 2007; Kositicin et al, 2014a.|ca 1050 Ma to 1000 Ma (Camacho et al, 2002)|||Equivalent to the Yackah beds. Overlain by the Bitter Springs Group.||
8223|Heavitree Formation|72601|6|Mentioned|p3, p7|Tonian|Tonian|Amadeus Basin. Found in the northern part of the basin. Previously called the Heavitree Sandstone.||||Overlain by Gillen Formation (Bitter Springs Group).||
8223|Heavitree Formation|72714|6|Mentioned|p2, p4, p16-17|||Amadeus Basin. Regionally, copper-bearing fluorite veins are found on the contact between the Atneequa Suite and overlying Heavitree Formation and Bitter Springs Group.||||||
8223|Heavitree Formation|73085|6|Mentioned|p1|Tonian|Tonian|Previously called Heavitree Quartzite.||||Overlain by Gillen Formation (Bitter Springs Group). Equivalent to Dean Quartzite.||
8223|Heavitree Formation|73086|1|Redefined|[See comments]|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Re-definition and assignment of type area of undivided Heavitree Formation, change of name from quartzite to formation. Updated to formation to reflect the more varied nature of component sandstone (metamorphism isn't ubiquitous). Complex lithofacies associations are used to delineate four members in the Alice Springs region. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Thickness: 100-300 m [authors note that previous maximum thicknesses of 440 m may be in error due to complex folding]. No fossils or trace fossils. Geochron is detrital zircon maximum depositional age (MDA) and a range of 1050-1000 Ma is reported. Minimum age of deposition is ca 820 Ma based on overlying units. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. Correlates to Dean, Vaughan Springs, Amesbury, and Stanovos quartzites, Yakah beds, and Munyu Sandstone. Possibly correlates to Kulail Sandstone. Previous names also include No 1 quartzite [also written as No. 1 quartzite], No 1 Ridge quartzite [also written as No. 1 Ridge quartzite], and Heavitree Range quartzite [see p. 9, 44]. p: 3-15, 18-19, 25, 30, 39, 44, 57, 60, ~62-66, 103, 105, 114, 130, 143-147, 150, App 2.|1050-1000 Ma max depositional age||Undoolya Member, Temple Bar Member, Fenn Gap Member, Blatherskite Member|Underlain by Sadadeen Gneiss and Ingwallumum granite. Conformably overlain by Gillen Formation (Bitter Springs Group). Unconformably overlain by Wallara Formation. [See comments].|Comprises dominantly fine-grained, with lesser medium- to coarse-grained, planar- and cross-bedded, variably feldspathic sandstone that is predominantly silicified. Local laminated mudstone and conglomerate intervals are known.|
8223|Heavitree Formation|73088|6|Mentioned|p1-2, p4, p12|Tonian|Tonian|Amadeus Basin, northeast. Underlain by Palaeo-Mesoproterozoic basement. Previously called Heavitree Quartzite.||||Overlain by Gillen Formation (Bitter Springs Group).|Includes quartzite and siltstone.|
8223|Heavitree Formation|73338|6|Mentioned|p5, p8|Neoproterozoic|Neoproterozoic|Drilled to test for petroleum systems by Santos Ltd (Magee 1). Absent from Mount Kitty 1 well. Unconformably overlies crystalline basement in Magee 1.|||||Sandstone.|
8223|Heavitree Formation|73551|6|Mentioned|p21, p23|Stenian|Stenian|Maximum depositional ages of ca 1.12 Ga (Maidment, 2005), 1073 +/- 12 Ma (Normington et al., 2016), and 1050 +/- 10 Ma (Kositcin et al., 2013).|ca 1.1 Ga|||||
8238|Hebe Shale|38936|5|Briefly described|p336|||||||||
8259|Helicopter Siltstone|22547|3|Fully described|p27||Cryogenian|Victoria River Basin.  Age: c.800 Ma. Thickness: 330m. Overlies Ahern Formation, overlain by Moonlight Valley Tillite||||||26-SEP-06
8259|Helicopter Siltstone|22716|6|Mentioned|table4, p239|Ectasian|Ectasian|Overlying Lamboo Complex. Thought to be part of supersequence 1 of Centralian Superbasin||||||
8259|Helicopter Siltstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria River Basin.||||||
8259|Helicopter Siltstone|23314|6|Mentioned|333|||||||||
8259|Helicopter Siltstone|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Correlates with the Auvergne Group, and the Renner Group (Ashburton Province) and Roper Group (McArthur Basin).  Geological Province: Victoria Basin.||||||
8259|Helicopter Siltstone|24122|6|Mentioned|p1|||||||||
8259|Helicopter Siltstone|24297|6|Mentioned|p4|||||||||
8259|Helicopter Siltstone|24503|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria River Basin.||||||
8259|Helicopter Siltstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8259|Helicopter Siltstone|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8259|Helicopter Siltstone|32660|5|Briefly described|Table 6|||||||||
8259|Helicopter Siltstone|32701|6|Mentioned|p14|||Refers Dow and Gemuts (1969)||||||26-SEP-06
8259|Helicopter Siltstone|32728|6|Mentioned|Fig.3|||||||||
8259|Helicopter Siltstone|36551|6|Mentioned|Table 12|||||||||
8259|Helicopter Siltstone|36885|4|Described|p177|||||||||
8259|Helicopter Siltstone|36898|6|Mentioned|p184|||||||||
8259|Helicopter Siltstone|37462|4|Described|Table 4.VI|||||||||
8259|Helicopter Siltstone|38157|6|Mentioned|Table X|||||||||
8259|Helicopter Siltstone|38988|6|Mentioned|Fig.4|||||||||
8259|Helicopter Siltstone|43853|5|Briefly described|Map Legend||Proterozoic|||||||
8259|Helicopter Siltstone|43855|5|Briefly described|Map Legend||Proterozoic|||||||
8259|Helicopter Siltstone|44155|4|Described|p251-252|||165m thick. Poorly exposed in the valley of Fargoo Creek.||||Overlies Wade Creek Sandstone conformably (gradationally).|Laminated khaki siltstone and shale; some fine-grained quartz sandstone.|
8259|Helicopter Siltstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
8259|Helicopter Siltstone|44317|4|Described|Table 3||Adelaidean|||||||
8259|Helicopter Siltstone|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
8259|Helicopter Siltstone|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
8259|Helicopter Siltstone|45047|2|Defined|p81|Adelaidean|Adelaidean|See also p82,33,35..||||||26-SEP-06
8259|Helicopter Siltstone|45112|6|Mentioned|Table 16|||||||||
8259|Helicopter Siltstone|45140|6|Mentioned|p59|||||||Gradationally overlies Wade Creek Sandstone. Is overlain unconformably by Redbank Yard Formation (Duerdin Group).||
8259|Helicopter Siltstone|48927|6|Mentioned|p6|||Refers Dow and Gemuts (1969)||||||26-SEP-06
8259|Helicopter Siltstone|48938|6|Mentioned|p76|||Correlation with Angalarri Silst.||||||
8259|Helicopter Siltstone|60682|5|Briefly described|p6|||Correlated with Angalarri Siltstone.||||||
8259|Helicopter Siltstone|60685|6|Mentioned|p4|||Mentioned in the context of the Ahernn Formation-Helicopter Siltstone possible correlated with Jasper Gorge Sandstone-Angalarri Siltstone.||||||26-SEP-06
8259|Helicopter Siltstone|63866|5|Briefly described|p130|||Victoria River Basin.||||||
8259|Helicopter Siltstone|64104|6|Mentioned|p63 Fig.1, p75, p76 fig 10, p77 fig 11|Neoproterozoic|Neoproterozoic|Osmond Basin. Uppermost unit of the Osmond Range succession.||||Is overlain by Duerdin Group.||
8259|Helicopter Siltstone|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.||||||09-DEC-08
8259|Helicopter Siltstone|65413|6|Mentioned|p104.|||||||Faulted against McHale Granodiorite.||
8259|Helicopter Siltstone|65417|6|Mentioned|p158 Fig.2, p159.|Neoproterozoic|Neoproterozoic|Western Victoria River Basin. With upper Wade Creek Sandstone, is equivalent to the Auvergne Group (Victoria River Basin).||||Overlies the upper part of Wade Creek Sandstone.||
8259|Helicopter Siltstone|68244|6|Mentioned|p669|||Victoria River Basin.||||Overlain unconformably by Duerdin Group.||
8259|Helicopter Siltstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Neoproterozoic|Neoproterozoic|Victoria River Basin|||Includes unnamed member||green and grey micaceous siltstone, thin- to thick-bedded fine- to medium-grained quartz sandstone, and mudstone|
8259|Helicopter Siltstone|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 500k_interpgeop_lut.csv. |||||Grey and green micaceous siltstone, fine to medium grained quartz sandstone and mudstone.|
8259|Helicopter Siltstone|69634|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Of Victoria River Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1000-541 Ma (Inferred)||||Green and grey micaceous siltstone, fine- to medium-grained quartz sandstone, and mudstone|
8259|Helicopter Siltstone|70154|4|Described|100k_interpgeop_lut.csv|Cryogenian|Cryogenian|See also 500k_interpgeop_lut.csv.|635-850 Ma||||Micaceous siltstone, fine-coarse grained quartz sandstone, mudstone|
8259|Helicopter Siltstone|71267|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Victoria Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1000-720 Ma (inferred)||||Green and grey micaceous siltstone, fine- to medium-grained quartz sandstone, and mudstone|
8259|Helicopter Siltstone|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Victoria Basin.|||||Green and grey micaceous siltstone, fine- to medium-grained quartz sandstone, and mudstone.|
8259|Helicopter Siltstone|73255|6|Mentioned|p534 Fig.2, p548 Fig.12|Cryogenian|Cryogenian|||Osmond Range Succession||Overlies the Wade Sandstone, disconformably underlies the Fargoo Tillite.||
8272|Henry River Formation|29845|6|Mentioned|Table 69|||||||||
8274|Henry-Telfer Granite|40089|6|Mentioned|p71|||||||||
8279|Hensman Sandstone|22547|4|Described|p24||Mesoproterozoic|Of the Carr Boyd Group.  Geological Province: Carr Boyd Basin. Thickness: 120m. Overlies Revolver Creek Formation, overlain by Golden Gate Siltstone||||||26-SEP-06
8279|Hensman Sandstone|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Carr Boyd Group||||||
8279|Hensman Sandstone|30097|6|Mentioned|Table 23|||Also Table 24||||||
8279|Hensman Sandstone|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8279|Hensman Sandstone|32660|5|Briefly described|Table 6|||||||||
8279|Hensman Sandstone|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
8279|Hensman Sandstone|32728|5|Briefly described|Table 6|||See also P46||||||
8279|Hensman Sandstone|36551|6|Mentioned|Table 12|||||||||
8279|Hensman Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
8279|Hensman Sandstone|41158|5|Briefly described|p39|||Of the Carr Boyd Group. Massive silicified quartz sandstone.  Overlain by Golden Gate Siltstone.||||||28-SEP-06
8279|Hensman Sandstone|42191|5|Briefly described|Fig.7 P140|||||||||
8279|Hensman Sandstone|43853|5|Briefly described|Map Legend||Proterozoic|||||||
8279|Hensman Sandstone|44155|5|Briefly described|p250 Tb.3-10|||||Carr Boyd Group||Overlies Revolver Creek Formation unconformably.|Massive silicified fine- to medium-grained quartz sandstone.|
8279|Hensman Sandstone|44230|5|Briefly described|Map Legend||Proterozoic|||||||
8279|Hensman Sandstone|44363|5|Briefly described|p.6,11,15,17,24,28|||(Adelaidean). Of the Carr Boyd Group.||||||28-SEP-06
8279|Hensman Sandstone|44364|14|Not recorded|map legend||Proterozoic|||||||
8279|Hensman Sandstone|45047|4|Described|p35|||Of Carr Boyd Group.||||||28-SEP-06
8279|Hensman Sandstone|45112|6|Mentioned|Table 16|||||||||
8279|Hensman Sandstone|48938|6|Mentioned|p9|||Stratigraphy.||||||
8279|Hensman Sandstone|65417|5|Briefly described|pp156-159.|Mesoproterozoic|Mesoproterozoic|Halls Creek Orogen. Transgressive shoreface sands.||Basal unit in Carr Boyd Group.||Is overlain conformably by Golden Gate Siltstone.||
8279|Hensman Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Carr Boyd Basin||Carr Boyd Group|||Fine- to coarse-grained quartz sandstone, heavily silicified.|31-JUL-15
8279|Hensman Sandstone|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||||||Fine to coarse grained quartz sandstone, heavily silicified.|
8279|Hensman Sandstone|69435|5|Briefly described|p20:3|||Carr Boyd Basin.||Carr Boyd Group.||Is overlain by Golden Gate Siltstone.||12-JUL-16
8279|Hensman Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.|1200-1177 Ma (Inferred)|Unit of Carr Boyd Group.|||Fine- to coarse-grained quartz sandstone, heavily silicified|
8279|Hensman Sandstone|69673|6|Mentioned|p60 fig 48|||||Carr Boyd Group||Overlain by Golden Gate Siltstone||
8279|Hensman Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic||1177-1200 Ma|Carr Boyd Group|||Fine to coarse grained quartz sandstone, heavily silicified.|
8279|Hensman Sandstone|70812|5|Briefly described|p23|Middle Proterozoic|Middle Proterozoic|||||||
8279|Hensman Sandstone|71267|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Carr Boyd Basin. Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|1200-1177 Ma (inferred)|Unit of Carr Boyd Group.|||Fine- to coarse-grained, massive quartz sandstone, heavily silicified|
8300|Herschel Limestone|42473|6|Mentioned|p35|||Misspelling of Herschell Limestone?||||||
8324|Hicks Range Sandstone Member|22741|5|Briefly described|p29, Table3 p12||Late Permian|||||||10-FEB-20
8324|Hicks Range Sandstone Member|22767|5|Briefly described|Table3 p14, p22||Late Permian|||||||10-FEB-20
8324|Hicks Range Sandstone Member|22776|4|Described|Table.3|Late Permian|Late Permian|Hardman Formation, Liveringa Group||||||
8324|Hicks Range Sandstone Member|30342|6|Mentioned|Table 2|||||||||
8324|Hicks Range Sandstone Member|33518|4|Described|Table 1|||||||||
8324|Hicks Range Sandstone Member|33519|6|Mentioned|Map legend|Permian|Permian|||||||
8324|Hicks Range Sandstone Member|33962|2|Defined|p51|Permian|Permian|||||||
8324|Hicks Range Sandstone Member|36224|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Hardman Formation.||||||01-FEB-05
8324|Hicks Range Sandstone Member|36225|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
8324|Hicks Range Sandstone Member|36634|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
8324|Hicks Range Sandstone Member|41540|5|Briefly described|p21|||||||||
8324|Hicks Range Sandstone Member|41688|6|Mentioned|p10|||||||||
8324|Hicks Range Sandstone Member|45153|6|Mentioned|App.4-73|||See also App.4-77||||||
8324|Hicks Range Sandstone Member|45158|4|Described|p18|||||||||
8324|Hicks Range Sandstone Member|66949|5|Briefly described|p56 Appx.3|Wuchiapingian|Wuchiapingian|[Superseded]. See also Hicks Range Member (p4 Fig.2, p25). Type section detailed. Up to 325m thick [25 m in type section]; fluvial deposits. Biostratigraphic zonation.||Unit in Hardman Formation.||Overlies Kirkby Range Member. Is overlain by Cherrabun Member.|Sandstone.|04-NOV-15
8332|High Cliff Sandstone|12758|5|Briefly described|p8 Fig. 9|Permian|Permian|Geological Province: Northern Perth Basin.||||||
8332|High Cliff Sandstone|14227|5|Briefly described|p7|Permian|Permian|Also presented as Highcliff Sandstone - both forms of the name used interchangeably. Marine sands. Geological province: Perth Basin. See also Enclosure 2.||||||07-FEB-11
8332|High Cliff Sandstone|15881|5|Briefly described|p62|||Overlay Fossil Cliff Formation (Playford et al 1975).||||||
8332|High Cliff Sandstone|22820|6|Mentioned|p16|||Geological province: northern Perth Basin. Readily correlates with Woodynook Sandstone (Sue Group) in southern Perth Basin, and Westralia Sandstone in the Collie Basin||||||11-AUG-08
8332|High Cliff Sandstone|23172|4|Described|Map Legend|Permian|Permian|||||||
8332|High Cliff Sandstone|23174|3|Fully described|6,Fig5p8,10|Early Permian|Early Permian|||||||
8332|High Cliff Sandstone|23279|4|Described|p12-4,Fig2p3||Artinskian|(Clarke et al., 1951).||||||
8332|High Cliff Sandstone|23520|5|Briefly described|p11 Fig. 7|Artinskian|Sakmarian|Geological Province: Perth Basin. See also p16.||||||27-JUL-09
8332|High Cliff Sandstone|23761|5|Briefly described|p11|||||||||
8332|High Cliff Sandstone|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||23-DEC-09
8332|High Cliff Sandstone|23816|4|Described|p233|Artinskian|Artinskian|Age: Early Artinskian. Geological Province: Perth Basin. Conformably underlain by Fossil Cliff Formation; conformably overlain by Irwin River Coal Measures. Max. thickness: 31 m. Richly fossiliferous.||||||18-OCT-07
8332|High Cliff Sandstone|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
8332|High Cliff Sandstone|24390|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Perth Basin.||||||
8332|High Cliff Sandstone|24443|5|Briefly described|Fig.30|Early Permian|Early Permian|Conformably overlies Holmwood Shale. Conformably overlain by Irwin River Coal Measures. Geological Province: Bight Basin.||||||
8332|High Cliff Sandstone|29548|6|Mentioned|p230|||Permian.||||||
8332|High Cliff Sandstone|30545|6|Mentioned|p22|||Lower Permian.||||||
8332|High Cliff Sandstone|30948|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
8332|High Cliff Sandstone|30973|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
8332|High Cliff Sandstone|31394|5|Briefly described|Fig.4|||L.Permian||||||
8332|High Cliff Sandstone|31561|6|Mentioned|p18|||Stratigraphic column||||||
8332|High Cliff Sandstone|31910|5|Briefly described|Table 1|||p17.||||||18-OCT-07
8332|High Cliff Sandstone|32165|6|Mentioned|p196|||Sections correlated BMR10 & 10A||||||
8332|High Cliff Sandstone|32337|4|Described|p25|||||||||
8332|High Cliff Sandstone|32648|6|Mentioned|p32|||L. Perm.||||||
8332|High Cliff Sandstone|32649|4|Described|p23|||See also Table 1||||||
8332|High Cliff Sandstone|32840|6|Mentioned|Table 1|||||||||
8332|High Cliff Sandstone|32945|6|Mentioned|p88|||See also p73. Sakmarian||||||18-OCT-07
8332|High Cliff Sandstone|33022|6|Mentioned|p261|||Palaeomagnetism||||||
8332|High Cliff Sandstone|33052|6|Mentioned|Fig.1|||Artinskian||||||
8332|High Cliff Sandstone|33701|6|Mentioned|Fig.1|||Artinskian||||||
8332|High Cliff Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
8332|High Cliff Sandstone|34532|6|Mentioned|p226|||See also Fig.2||||||
8332|High Cliff Sandstone|34570|6|Mentioned|p115|||||||||
8332|High Cliff Sandstone|35282|6|Mentioned|p35|||||||||
8332|High Cliff Sandstone|35873|6|Mentioned|p92|||||||||
8332|High Cliff Sandstone|36020|6|Mentioned|p388|||||||||
8332|High Cliff Sandstone|36257|6|Mentioned|Table 2.1|||||||||
8332|High Cliff Sandstone|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological Province: Perth Basin.||||||21-APR-08
8332|High Cliff Sandstone|36293|2|Defined|p97|Permian|Permian|||||||
8332|High Cliff Sandstone|36890|3|Fully described|p233|||||||||
8332|High Cliff Sandstone|36899|6|Mentioned|Fig.3|||||||||
8332|High Cliff Sandstone|37104|6|Mentioned|Fig.3|||||||||
8332|High Cliff Sandstone|37298|6|Mentioned|Fig.1|||||||||
8332|High Cliff Sandstone|38917|6|Mentioned|p169|||||||||
8332|High Cliff Sandstone|38998|4|Described|p20|||||||||
8332|High Cliff Sandstone|40340|5|Briefly described|p13|||||||||
8332|High Cliff Sandstone|40341|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
8332|High Cliff Sandstone|40342|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
8332|High Cliff Sandstone|40343|5|Briefly described|p10|||||||||
8332|High Cliff Sandstone|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8332|High Cliff Sandstone|40347|5|Briefly described|p23|||||||||
8332|High Cliff Sandstone|40992|6|Mentioned|Fig.5|||||||||
8332|High Cliff Sandstone|41514|6|Mentioned|p62|||||||||
8332|High Cliff Sandstone|41728|6|Mentioned|Fig.2|||||||||
8332|High Cliff Sandstone|42309|6|Mentioned|p256|||||||||
8332|High Cliff Sandstone|42462|6|Mentioned|p63|||In the Perth Basin.||||||18-OCT-07
8332|High Cliff Sandstone|42654|6|Mentioned|p14|||||||||
8332|High Cliff Sandstone|42711|6|Mentioned|p23|||Geological province: northern Perth Basin. Equivalent to Westralia Sandstone of the Collie Group in the Collie Basin.||||||
8332|High Cliff Sandstone|43015|5|Briefly described|Table 1,p319|||||||||
8332|High Cliff Sandstone|43018|5|Briefly described|Table 1,p386|||||||||
8332|High Cliff Sandstone|43031|5|Briefly described|Fig,2.|||||||||
8332|High Cliff Sandstone|43050|5|Briefly described|p8|||||||||
8332|High Cliff Sandstone|43067|5|Briefly described|Fig.12,p124|||||||||
8332|High Cliff Sandstone|43216|5|Briefly described|Map Legend||Permian|In the Perth Basin.||||||18-OCT-07
8332|High Cliff Sandstone|43217|5|Briefly described|Map Legend||Permian|In the Perth Basin.||||||18-OCT-07
8332|High Cliff Sandstone|43296|6|Mentioned|Map Legend||Permian|||||||
8332|High Cliff Sandstone|43297|4|Described|p4, fig.3 p5||Artinskian|Type section location given. Also Table1 p7.||||||
8332|High Cliff Sandstone|43347|6|Mentioned|13|||||||||
8332|High Cliff Sandstone|43495|4|Described|6-32||Artinskian|||||||
8332|High Cliff Sandstone|43504|4|Described|4-9||Artinskian|||||||
8332|High Cliff Sandstone|44144|4|Described|p508 Tb.4-21, p509 Fig.4-145, p510-512|Artinskian|Artinskian|Type Section: High Cliff; 28o56'40''S 115o32'45''E. 42m thick shallow marine or shoreline deposits.||||Conformably overlies Holmwood Shale. Overlain conformably by Irwin River Coal Measures.|Fine-grained quartz sandstone with interbeds of coarse-grained sandstone, conglomerate and siltstone.|
8332|High Cliff Sandstone|44219|14|Not recorded|p31||Artinskian|||||||
8332|High Cliff Sandstone|44994|6|Mentioned|Fig.7|||Permian. Correlation.||||||
8332|High Cliff Sandstone|45001|14|Not recorded|p7|Artinskian|Artinskian|||||||25-NOV-16
8332|High Cliff Sandstone|45016|14|Not recorded|p..87,112|||Probably correlates with Moogooloo Sandstone.||||||
8332|High Cliff Sandstone|45168|6|Mentioned|p6|||||||||
8332|High Cliff Sandstone|46849|6|Mentioned|Fig. 6|||||||||
8332|High Cliff Sandstone|48615|14|Not recorded|p.1,3,4,5,11,13,14.|||(H50-1,9). On many pages. Fig.2. Pl.2.||||||
8332|High Cliff Sandstone|48848|14|Not recorded|p.79,89|||||||||
8332|High Cliff Sandstone|49644|5|Briefly described|Table|||||||||
8332|High Cliff Sandstone|50085|5|Briefly described|p15 Fig. 8|Permian|Permian|Geological Province: Northern Perth Basin.||||||11-MAY-04
8332|High Cliff Sandstone|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
8332|High Cliff Sandstone|60376|5|Briefly described|p17 Fig. 4.|Early Permian|Early Permian|Geological Province: Perth Basin. Overlain by Irwin River Coal Measures. Underlain by Holmwood Shale. Sandstone is SST in text.||||||07-FEB-11
8332|High Cliff Sandstone|60377|5|Briefly described|p61 Fig. 3, p72|Artinskian|Sakmarian|Overlain by Irwin River Coal Measures. Underlain by Holmwood Shale. Geological Province: Perth Basin. Depositional Environment is shoreface.||||||07-FEB-11
8332|High Cliff Sandstone|60386|5|Briefly described|p297, p309|Artinskian|Artinskian|Northern Perth Basin. Non-marine and deltaic - nearshore - shelf. ||||||
8332|High Cliff Sandstone|61023|5|Briefly described|p20 Fig 10|Permian|Permian|Geological Province: Perth Basin.||||||11-APR-08
8332|High Cliff Sandstone|61546|5|Briefly described|p382, p385 Fig.5, p386, p392. |Early Permian|Early Permian|Cliff Head oil field, Perth Basin. 70 to 100m thick. 6-18% porosity varying with quartz cementation. Deposited in an upper shoreface to foreshore environment.||||Overlies Holmwood Shale. Is overlain by Irwin River Coal Measures.|Massive clean sandstone.|
8332|High Cliff Sandstone|61811|4|Described|p3 Fig.2, p36, pp38-45, p63.|Artinskian|Sakmarian|Northern Perth Basin. 24 m thick at type section: High Cliff on the North Branch of the Irwin River; further details in Appendix 1.||||Conformably overlies Holmwood Shale. Is overlain conformably by Irwin River Coal Measures.|Siliciclastic paralic deposits: white and red, feldspathic, cross-bedded and bioturbated sandstone, interbedded with conglomerate and siltstone.|
8332|High Cliff Sandstone|62113|3|Fully described|pp618-621, pp625-627, p630.     |Artinskian|Artinskian|Coarse-grained regressive marine succession up to 116m thick in the subsurface and 26m thick at its type section at High Cliff on the North Branch of the Irwin River. Deposited in a storm-influenced inner shelf setting on the outer margins of coalesced fan deltas; palaeocurrents predominantly to south and southeast. Has a shallow-marine assemblage of gastropods, bivalves and brachiopods. Late Sakmarian - early Artinskian Striatopodocarpites fusus zone suggested by Backhouse (1993). Low hydrocarbon generation potential.|<290 Ma.|||Unconformably overlies the Holmwood Shale. Is overlain conformably by the Irwin River Coal Measures.|Sandstone and mudstone. Type section shows a coarsening-upwards succession of cross-bedded and bioturbated sandstone with several thin conglomeratic horizons.|
8332|High Cliff Sandstone|64580|4|Described|map legend||Early Permian|Fine-grained quartz sandstone, subordinate interbeds of coarse-grained sandstone, conglomerate and shale.||||||09-DEC-08
8332|High Cliff Sandstone|64630|5|Briefly described|p31 Fig.2, p34|Artinskian|Sakmarian|Province: Northern Perth Basin. Underlies the Irwin River Coal Measures, overlies the Holmwood Shale. Palynology age: P. pseudoreticulata to D. byroensis.||||||24-NOV-09
8332|High Cliff Sandstone|64635|5|Briefly described|p4 Fig.3, p18-26        |Artinskian|Sakmarian|Of Clarke et al. (1954). Siliciclastic paralic deposits. Type section is at High Cliff on the North Branch of the Irwin River. Diagram of the type section p21 Fig.18.||||Conformably overlies the Fossil Cliff Member (Holmwood Shale). Conformably overlain by the Irwin River Coal Measures.|Interbedded sandstone, conglomerate and siltstone. 24 m thick at the type section.|
8332|High Cliff Sandstone|64972|6|Mentioned|p617 Fig. 5|Early Permian|Early Permian|Geological Province: Perth Basin.||||||
8332|High Cliff Sandstone|64974|6|Mentioned|p143, p144 Fig. 3|Artinskian|Artinskian|Geological Province: Perth Basin.||||||24-JUN-09
8332|High Cliff Sandstone|67135|5|Briefly described|p5 Fig.7.|Permian|Permian|Perth Basin.||||Overlies Nangetty Formation. Is overlain by Irwin River and Sue Coal Measures.||
8332|High Cliff Sandstone|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.||||||
8332|High Cliff Sandstone|67925|5|Briefly described|Ch4 p8 fig 2|Lower Permian|Lower Permian|Northern and central Perth Basin. ||||Overlies the HolmWood Shale. Overlain by the Irwin River Coal Measures.||
8332|High Cliff Sandstone|67977|5|Briefly described|p479, p491|Sakmarian|Sakmarian|Geol. Prov: northern Perth Basin||||||
8332|High Cliff Sandstone|69029|6|Mentioned|p332|Artinskian|Artinskian|Of Perth Basin.||||Overlain by Rosabrook Coal Measures. Underlain by Woodynook Sandstone.||
8332|High Cliff Sandstone|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p11, Ch2 p34-p41|Early Permian|Early Permian|Perth Basin. Deposited in a shore-face or shoreline environment. Contains oil and gas and is generally a good reservoir with porosity >10 percent and permeability more than 10mD; however it lacks a proper seal. See also  Ch2 p44-p49, Ch2 p54-p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p70, Ch2 p73, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100-p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||||Overlies the Holmwood Shale. Overlain by the Irwin River Coal Measures and the Sue Group.|Massively bedded, well sorted and fine to medium-grained sandstone.|
8332|High Cliff Sandstone|69547|4|Described|p182,192-193,197|Artinskian|Artinskian|northern Perth Basin. Type section: 3 km west of the Darling Fault that bounds the basin (see Eyles et al., 2006). Depositional environment: Shoreface to marginal marine facies. Glacially-influenced succession, and correlable with Winnamea Sandstone and Ballythanna Sandstone. Progradational facies over Holmwood Shale and is a transitional unit between the underlying Holmwood Shale and overlying Irwin River Coal Measures.||||Underlain by Holmwood Shale. Overlain by Irwin River Coal Measures.||
8332|High Cliff Sandstone|69583|5|Briefly described|p130, Plate 3.|Paleozoic|Paleozoic|Perth Basin.|||||Fine-grained quartz sandstone, subordinate interbeds of coarse-grained sandstone, conglomerate and shale.|
8332|High Cliff Sandstone|70097|5|Briefly described|p2, p20 Fig.4|Sakmarian|Sakmarian|Northern Perth Basin. Irwin Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies Holmwood Shale. Is overlain by Irwin River Coal Measures.|Pro-glacial marine basin fill. Includes sandstone.|12-SEP-17
8332|High Cliff Sandstone|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Holmwood Shale. Is overlain conformably by Irwin River Coal Measures.||
8332|High Cliff Sandstone|70774|5|Briefly described|p5 fig 3|Artinskian|Sakmarian|Northern Perth Basin.||||Overlies the Holmwood Shale. Overlain by the Irwin River Coal Measures.||
8332|High Cliff Sandstone|70796|5|Briefly described|500k_interpgeop14_lut.csv|Artinskian|Artinskian|Perth Basin. Formed during Gondwana breakup along the western margin.|290.1  283.5 Ma (biostrat)||||Finegrained quartz sandstone, subordinate interbeds of coarsegrained sandstone, conglomerate, and shale|
8332|High Cliff Sandstone|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Perth Basin.||||||
8332|High Cliff Sandstone|71146|5|Briefly described|p6,  p43 fig 33|Artinskian|Sakmarian|Perth Basin.||||Overlies the Holmwood Shale. Overlain by the Irwin River Coal Measures.|Sandstone, conglomerate, carbonate and mudstone.|
8332|High Cliff Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, claystone, shale, sandstone|
8332|High Cliff Sandstone|71269|4|Described|GEOL_LUT_CSV files|Artinskian|Artinskian|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??.  See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv. |290.1-283.5 Ma (biostrat)||||Fine-grained quartz sandstone, subordinate interbeds of coarse-grained sandstone, conglomerate, and shale|
8332|High Cliff Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Artinskian|Artinskian|Perth Basin.  Age from biostratigraphy.||Permian package 1, Perth Basin.|||Fine-grained quartz sandstone, subordinate interbeds of coarse-grained sandstone, conglomerate, and shale.|
8332|High Cliff Sandstone|72258|5|Briefly described|p129,133|Cisuralian|Cisuralian|Of Perth Basin. Neoarchean (2800-2600 Ma) detrital zircons attributed to Yilgarn Craton, along eastern boundary of Perth Basin (Kositcin et al., 2008; Mole et al., 2013; Nemchin and Pidgeon, 1997). Older material (3700-3000 Ma) probably also derived from Yilgarn Craton.||||Overlain by Irwin River Coal Measures. Underlain by Holmwood Shale. Laterally grades into Rosabrook Coal Measures.||
8332|High Cliff Sandstone|72505|5|Briefly described|p890|Artinskian|Sakmarian|Perth Basin. Correlated with the Stratopodocarpites fusus zone and the Pseudoreticulosporta pseudoreticulata zone.||||Overlies the Holmwood Shale. Overlain by the Irwin River Coal Measures.||
8332|High Cliff Sandstone|72910|6|Mentioned|p4 Fig.3.|Sakmarian|Sakmarian|Shown as part of the Northern Perth Basin.||||Overlies Holmwood  Shale and underlies Irwin River Coal Measures. Laterally equivalent in part to Callytharra Formation.||
8332|High Cliff Sandstone|73117|6|Mentioned|p15|Artinskian|Asselian|||||Underlain by Holmwood Shale. Overlain by and equivalent to[?] 'Kingia Sandstone'.||
8332|High Cliff Sandstone|73484|5|Briefly described|p476 Fig.3|Cisuralian|Cisuralian|Perth Basin. Marine sands.||||Overlies Holmwood Shale, underlies Irwin River Coal Measures||
8332|High Cliff Sandstone|73513|4|Described|p29, p30 Fig.2, p31-33, p35-38, p40-41|Artinskian|Sakmarian|Perth Basin. Typically 50-150 m thick in subsurface, 200 m thick in Waitsia area, 26 m thick in outcrop type section. Thickest in the northeast, thins to the south and west. Deposited in a shoreface setting. Reservoir for the Waitsia Field.|||Bit Basher Shale, Kingia Sandstone|Overlies Holmwood Shale with abrupt transition, underlies Irwin River Coal Measures with transitional boundary|Dominated by thick beds of quartzose sandstone with minor siltstone interbeds. Includes sandstone with minor conglomerate and siltstone, medium grained and medium-well sorted with quartz arenite to sub-arkose composition.|
8332|High Cliff Sandstone|73623|5|Briefly described|p4, 6, 16|Cisuralian|Cisuralian|Irwin Basin. Represents a progradational phase with the influx of quartz sand.||||Overlies Holmwood Shale. Is overlain by Irwin River Coal Measures.||
8341|Hilda Rhyolite|30388|4|Described|p9|||See also P10. Middle Proterozoic age.||||||
8341|Hilda Rhyolite|30390|4|Described|p58|||||||||
8341|Hilda Rhyolite|30884|6|Mentioned|p159|||||||||
8341|Hilda Rhyolite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8341|Hilda Rhyolite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8341|Hilda Rhyolite|36551|6|Mentioned|Table 31|||||||||
8341|Hilda Rhyolite|36886|4|Described|p198|||||||||
8341|Hilda Rhyolite|40089|6|Mentioned|Table 29|||||||||
8341|Hilda Rhyolite|50607|5|Briefly described|p3.2|||Of the Bentley Supergroup. Geological Province: Musgrave Block.||||||
8341|Hilda Rhyolite|67375|5|Briefly described|p38 Table 1. |Mesoproterozoic|Mesoproterozoic|||Unit in Cassidy Group.||Overlies Warubuyu Basalt. Is overlain by Miller Basalt.|Dark-grey, feldspar-phyric rhyolite with very fine-grained groundmass; massive, flow-banded or spherulitic|
8341|Hilda Rhyolite|67553|5|Briefly described|p40,51|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of Talbot Sub-basin, Bentley Sub-basin.||Unit of Cassidy Group.||Overlain by Miller Basalt. Underlain by .Warubuyu Basalt||
8341|Hilda Rhyolite|68995|5|Briefly described|p7 Fig.3, p9 Tb. 1, p18|Stenian|Stenian|Estimated 590m thick. Outcrops over 65km from the Warburton area eastward where it thins out. Metamorphism discussed. Misspelt as the Hilda rhyolite on p61. See also p19, p22, p25, p27 Tb.2, p56, p61.||Cassidy Group||Overlies the Warubuyu Basalt. Overlain by the Miller Basalt.|Rhyolitic lava flows or rheomorphic ignimbrites.|
8341|Hilda Rhyolite|69091|6|Mentioned|p71 Fig.4.14|||Talbot Sub-basin||Cassidy Group||||
8341|Hilda Rhyolite|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Mentioned in GEOCHRON/174691.1.pdf and 174690.1.pdf.||Cassidy Group|||Massive, spherulitic or porphyritic rhyolite; minor trachyte and dacite; vitric lavas|
8341|Hilda Rhyolite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Cassidy Group.||||
8341|Hilda Rhyolite|70095|5|Briefly described|p16-17,19|||Geological province: Musgrave Province. Talbot Sub-basin, Of Bentley Basin. Thickness of rhyolitic package: 0.54km, over 65km strike length, with interpreted minimum volume of 1050km3 (potentially reflecting two separate volumes). See p19 Table 2 for U-Pb zircon data.||Unit of Cassidy Group.||Overlain by Miller Basalt. Underlain by Warubuyu Basalt.||
8341|Hilda Rhyolite|70137|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. The two facies are mapped separately.||Cassidy Group.||Overlies Warubuyu Basalt. Is overlain by Miller Basalt.|Porphyritic rhyolite with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; subhedral to euhedral alkali-feldspar phenocrysts; moderately crystal-rich autobrecciated rhyolite, up to 20% phenocrysts of feldspar.|
8341|Hilda Rhyolite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP dates from sample (185407.1.pdf)|1047 Ma - 1077 Ma (Inferred), 1071 Ma  (SHRIMP)|Cassidy Group|||Porphyritic and microcrystaline, crystal rich, autobrecciated rhyolite with minor trachyte and dacite; massive-flow banded vitric lavas; subhedral-euhedral alkali-feldspar phenocrysts; minor plagioclase and embayed bipyramidal quartz phenocrysts.|
8341|Hilda Rhyolite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 185407 (rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1071+\-5 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Porphyritic (in part authobrecciated) rhyolite with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas.|
8341|Hilda Rhyolite|71211|6|Mentioned|p216|||||Cassidy Group||||
8341|Hilda Rhyolite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 185407 (rhyolite) yielded a concordia age of 1071+\-5 Ma, interpeted as magmatic crystallisation age of rhyolite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Cassidy Group.|||Porphyritic rhyolite with minor trachyte and dacite; massive to flow-banded and locally spherulitic vitric lavas; microcrystalline, moderately crystal-rich, flow-banded, autobrecciated rhyolite.|
8341|Hilda Rhyolite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1071+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
8341|Hilda Rhyolite|72443|5|Briefly described|p738-739, p742, p748|||Talbot Sub-basin.|1010 +/- 20 to 1067 +/- 11 Ma (SHRIMP U-Pb)|Cassidy Group||||
8342|Hilfordy Formation|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
8342|Hilfordy Formation|32660|5|Briefly described|Table 3|||||||||
8342|Hilfordy Formation|32728|6|Mentioned|Table 5|||||||||
8342|Hilfordy Formation|36551|6|Mentioned|Table 10|||||||||
8342|Hilfordy Formation|36885|4|Described|p184|||||||||
8342|Hilfordy Formation|44140|5|Briefly described|p294 Tb.4-1|Paleoproterozoic|Paleoproterozoic|30 m thick.||Crowhurst Group||Conformably overlies Pentecost Sandstone. Is overlain conformably by Liga Shale.|Purple and white quartz sandstone with interbedded siltstone and shale, sandstone; glauconitic in places|07-MAR-18
8342|Hilfordy Formation|44231|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Quartz sandstone, ferruginous siltstone, and shale. Geological Province: Crowhurst Basin.||||||28-SEP-12
8342|Hilfordy Formation|44397|14|Not recorded|p.9,17, Table 2||Carpentarian|Kimberley Group. Defn. on Tech.File E/52-9.||||||
8342|Hilfordy Formation|44398|14|Not recorded|map legend||Carpentarian|||||||
8342|Hilfordy Formation|45047|5|Briefly described|p28|||Crowhurst Group.||||||
8342|Hilfordy Formation|61574|5|Briefly described|p690|Proterozoic|Proterozoic|Of the Crowhurst Group. Overlies Pentecost Sandstone (Kimberley Group.).||||||07-JAN-10
8342|Hilfordy Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Interbedded purple and white flaggy and blocky, partly glauconitic fine and coarse quartz sandstone, purple thinly flaggy ferruginous siltstone and purple laminated shale|
8352|Hills Cone Lamproite|41158|6|Mentioned|Table 50|||||||||
8360|Hillside Adamellite|37633|5|Briefly described|Plate 4|||||||||
8376|Hinckley Range Gabbro|30386|5|Briefly described|p14|||||||||
8376|Hinckley Range Gabbro|30389|4|Described|p13|||See also P15||||||
8376|Hinckley Range Gabbro|30390|4|Described|p146|||||||||
8376|Hinckley Range Gabbro|30391|6|Mentioned|p455|||||||||
8376|Hinckley Range Gabbro|35726|6|Mentioned|p102|||||||||
8376|Hinckley Range Gabbro|36886|4|Described|p203|||||||||
8376|Hinckley Range Gabbro|44139|5|Briefly described|p284, p285 Fig. 3-69|||Of Giles Complex. 2750m sequence of norite, gabbro.||||||
8376|Hinckley Range Gabbro|69153|6|Mentioned|Rocks.csv|||Sample descriptions; including fine grained mafic rock - possibly dolerite dyke OR outcrop of Hinckley Range Gabbro. See also misspelt Hinkley Gabbro.|||||Gabbro; hand specimen description: fine grained mafic rock with veinlets (<10cm long) of felsic material; also contains veins of psuedotachylite|23-MAR-16
8376|Hinckley Range Gabbro|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1073+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granulite.|
8410|Hodgson Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8410|Hodgson Sandstone|23404|5|Briefly described|p645|||||||||
8410|Hodgson Sandstone|23937|2|Defined|p79 App. 1, p40|Calymmian|Calymmian|Supersedes Hodgson Sandstone Member (Abner Sandstone).  Now of the Collara Subgroup (Roper Group).  Disconformably overlain by Munyi Member (Corcoran Sst); overlies the Jalboi Formation.  Max. thickness: 130m.   Geological Province: McArthur Basin.||||||
8410|Hodgson Sandstone|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
8410|Hodgson Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: grey to brown, mainly coarse-grained, medium to thick-bedded, lenticular thin quartz granule beds, planar and trough cross-beds, current ripples, pseudo-karstically weathered. Geol. Prov: McArthur Basin.||||||13-OCT-05
8410|Hodgson Sandstone|24050|3|Fully described|p49, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Formerly Hodgson Sandstone Member of the Abner Sandstone.  Of the Roper Group.  Thick to very thick-bedded, fine- to very coarse-grained quartz sandstone.  Overlies Jalboi Formation.  Max. thickness: 100m.||||||26-SEP-06
8410|Hodgson Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||23-DEC-09
8410|Hodgson Sandstone|24303|5|Briefly described|p61 Appendix|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: McArthur Basin. Correlative of upper part of Powell Formation. See also p24 Tb.4||||||
8410|Hodgson Sandstone|40701|5|Briefly described|p41|||||||||
8410|Hodgson Sandstone|41220|6|Mentioned|Fig.3|||||||||
8410|Hodgson Sandstone|44112|6|Mentioned|Fig11p30|||||||||
8410|Hodgson Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Quartz sandstone, grey to pink, mostly fine- to medium-grained, medium bedded, trough cross-stratified, ripple marks, mud rip-up clasts. Overlies Jalboi Fm; underlies Corcoran Fm.||||||15-FEB-05
8410|Hodgson Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Quartz sandstone: grey to pink, mostly fine to medium grained, medium bedded, trough cross-stratified.||||||
8410|Hodgson Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: grey to brown, mainly coarse-grained, medium to thick-bedded, lenticular thin quartz granule beds, planar and trough cross-beds, current ripples, pseudo-karstically weathered. Geol. Prov: McArthur Basin.||||||26-SEP-06
8410|Hodgson Sandstone|61560|6|Mentioned|p489|||||||||
8410|Hodgson Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
8410|Hodgson Sandstone|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
8410|Hodgson Sandstone|69430|4|Described|p15:3, 26-27, 29-30|Calymmian|Calymmian|Abbott et al. (2001). Previously the Hodgson Sandstone Member (of Abner Sandstone in the Roper River region) of Dunn (1963). McArthur Basin. The top of this unit was selected by Abbott et al. (2001) as the top of their Collara Subgroup. A resistant unit. 30-130m thick. Coastal tidal platform sediments.||Topmost Collara Subgroup.||Ovelies Jalboi Formation gradationally or locally ?disconformably (erosive contact). Is overlain by Munyi Member (Corcoran Formation) disconformably to conformably.|White to pink, fine to coarse, strongly trough cross-bedded quartz sandstone.|12-JUL-16
8410|Hodgson Sandstone|69673|6|Mentioned|p16 fig 13, p35, p36, p40|||Northwestern and Southern McArthur Basin. 30-130m thick.||Collara Subgroup||Disconformably overlain by Munyi Member, Conformably overlies Jalboi Sandstone||
8410|Hodgson Sandstone|70734|5|Briefly described|p14, 16|||McArthur Basin. Tidal platform sandstone.||Of Collara Subgroup||Overlies Jalboi Formation. Overlain by Corcoran Formation.||
8410|Hodgson Sandstone|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Jalboi Formation; overlain by Munyi Member (Corcoran Formation).|Sandstone.|
8410|Hodgson Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Hodgson. McArthur Basin.||||||
8410|Hodgson Sandstone|70968|2|Defined|p6, p39-40, p42, p46-51, p53, p55, p124|Calymmian|Calymmian|See also p126-128, p131, p140, p143. Sweet in Abbott et al. (2001), after Dunn (1963) who originally named it the Hodgson Sandstone Member (of Abner Sandstone). Raised to Formation rank by Abbott et al. (2001). Named after Hodgson River. The type section, 8km NNW of Mount Chapman, is at 408300mE 8392300mN in URAPUNGA sheet. Resistant, strongly jointed scarp-forming unit: crops out as strike ridges and mesas. Forms spectacular parakarstic landforms. Widely distributed throughout McArthur Basin. Lithology well described and illustrated. Thickness ranges from 7.7m to c.300m; c.100m thick at the type section. Tide-dominated shoreline to shallow-marine deposits. Detrital zircon diagram.||Collara Subgroup.||Gradationally overlies Jalboi Formation. Is overlain disconformably (locally conformably) by Munyi Member (Corcoran Formation).|Dominated by thick intervals of cross-bedded quartz sandstone, punctuated by minor thin intervals of siltstone and mudrock.|
8410|Hodgson Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. <30 - 266+ m thick. Coastal tidal platform deposits.||Collara Subgroup.||Conformably overlies Jalboi Formation. Is overlain conformably to disconformably by Munyi Member (Corcoran Formation).|White to pink, cross-bedded, fine to coarse quartz sandstone.|
8410|Hodgson Sandstone|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Jalboi Formation. Unconformably overlain by the Maiwok Subgroup.||
8410|Hodgson Sandstone|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
8410|Hodgson Sandstone|71893|4|Described|iii, p2-p5, p8, p24-p28|Calymmian|Statherian|McArthur Basin. Appears in Sweet in Abbott et al 2001, after Dunn 1963a. A maximum depositional age of 1600 +/- 21 Ma and a youngest individual age of 1595 +/- 26 Ma are provided.  Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided. A maximum age is derived from the underlying Showell Member dated at 1493 +/- 4 Ma and a minimum age of 1361 +/- 21 Ma is derived from Re-Os of the Wyworrie Member of the overlying Velkerri Formation. Partial equivalent to the Abner Sandstone.||Collara Subgroup||Gradationally (in places unconformably) overlies the Jalboi Formation. Disconformably (locally conformably) overlain by the Munyi Member (Corcoran Formation).|White to pink, fine- to coarse-grained, strongly trough cross-bedded quartz sandstone, deposited in a tide-dominated shoreline to shallow marine setting.|
8410|Hodgson Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Collara Subgroup||Overlies Jalboi Formation and underlies Corcoran Formation.||
8410|Hodgson Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Collara Subgroup, Roper Group||Underlain by Jalboi Formation. Overlain by Corcoran Formation (Maiwok Subgroup). Equivalent to Abner Sandstone.||
8410|Hodgson 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.||Collara Subgroup||Overlies Jalboi Formation and underlies Corcoran Formation and is laterally equivalent, in part, to Abner Sandstone.||
8410|Hodgson Sandstone|72919|6|Mentioned|p1, p95|||Equivalent to sample 2712852 from Morstone 1.||Roper Group||||
8410|Hodgson Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Jalboi Formation. Overlain by Corcoran Formation.||
8410|Hodgson Sandstone|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Jalboi Formation. Overlain by Munyi Member, Corcoran Formation, Maiwok Subgroup.|Includes tidal Sandstone.|
8415|Hogarth Formation|30386|4|Described|Table 1|||Table 1 p7. Proterozoic age.||||||17-MAY-07
8415|Hogarth Formation|30390|4|Described|p56|||||||||
8415|Hogarth Formation|30942|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Member of Tollu Group||||||
8415|Hogarth Formation|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8415|Hogarth Formation|36551|6|Mentioned|Table 31|||||||||
8415|Hogarth Formation|36886|4|Described|p199|||||||||
8415|Hogarth Formation|44109|5|Briefly described|p9, p117|Mesoproterozoic|Mesoproterozoic|Of the Tollu Group. Comprises mafic to intermediate volcanic rocks, including amygdaloidal types, tuffs and agglomerates.It is most likely that the 1026 +/- 26 Ma dacite, originally believed to be Smoke Hill Volcanics, represents a subvolcanic sill that intruded into the Smoke Hill Volcanics (either belonging to the Hogarth Formation, or to an event that post-dates this formation).||||||02-DEC-13
8415|Hogarth Formation|61154|5|Briefly described|p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of the Tollu Group (Bentley Supergroup). Mafic to intermediate volcanics, tuffs and agglomerates. Geological Province: Amadeus Basin.||||||
8415|Hogarth Formation|61339|5|Briefly described|Map legend|||Of the Bentley Supergroup. Mafic volcanics.||||||03-AUG-09
8415|Hogarth Formation|62989|6|Mentioned|p39|||Of the Tollu group in WA.||||||
8415|Hogarth Formation|64745|5|Briefly described|p376|||Uppermost unit of Tollu Group. Correlated with Wankari Volcanics.||||||
8415|Hogarth Formation|65135|5|Briefly described|p16|||Basic to intermediate lavas. Overlies Smoke Hill Volcanics. Outcrops south of the Blackstone intrusion within the core of a syncline.||||||
8415|Hogarth Formation|65256|5|Briefly described|p14-15, p31|||Of Tollu Group; overlies Smoke Hill Felsic Volcanics. Fine-grained mafic to intermediate vesicular volcanics, tuffs and agglomerates. Correlated with Wankari volcanics of Bloods Range Formation.||||||25-MAR-15
8415|Hogarth Formation|65833|5|Briefly described|p16|Stenian|Stenian|Of Tollu Group. Overlies Smoke Hill Volcanics. Basic to intermediate lavas. Mis-spelt as Hoggarth on p16.||||||
8415|Hogarth Formation|65906|4|Described|p2, p6, p8-9, p23|Neoproterzoic|Mesoproterozoic|Mafic and intermediate volcanic rocks. Part of the Tollu Group. Overlies the Smoke Hill Volcanics. Correlative of Wankari Volcanics (Tjauwata Group).||||||
8415|Hogarth Formation|66281|5|Briefly described|Map legend|||Bentley Basin.||Unit in Tollu Group.|||Andesite, trachyandesite, trachyte, dacite; laminated felsic volcanic siltstone and lesser sandstone; felsic volcanic-pebble breccia.|
8415|Hogarth Formation|67128|5|Briefly described|p5 Fig.3, p11, p30|||Western Musgrave Province.||Tollu Group.||Conformably overlies Smoke Hill Volcanics. Is intruded by the Warakurna Supersuite.|Andesitic to trachytic lavas with rare basalt, trachyandesite, dacite, and fine- to coarse-grained volcaniclastic rocks. Lavas are typically variolitic and amygdaloidal.|
8415|Hogarth Formation|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin. Mapped as 6 separate but un-named units.|1073 - 1068 Ma.|Unit in Tollu Group.|||Andesitic to trachytic lavas; rare trachyandesite to dacite; laminated felsic volcanic siltstone and lesser sandstone; porphyritic aphanitic rhyolite; felsic volcanic-pebble breccia; metagabbro, massive with sub-ophitic texture.|
8415|Hogarth Formation|67375|5|Briefly described|p19, p38 Table 1, p40, p299, pp318-331.|Mesoproterozoic|Mesoproterozoic|The upper part of the redefined (Smithies et al. 2009) Tollu Group. Forms scattered and poor outcrop in the core of the Blackstone syncline.|1073-1026 Ma.|Unit in Tollu Group.|||Trachyandesite and trachydacite; pebble breccias, laminated volcanic siltstones and subordinate sandstones are interbedded with the lavas near the base of the Formation; porphyritic aphanitic rhyolite and lesser dacite lavas often occur near the top|
8415|Hogarth Formation|67553|5|Briefly described|p20,40,42-43,87-88|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Of  Blackstone Sub-basin, Bentley Sub-basin. Deposition constrained between the 1073+\-7 Ma maximum depositional age of the Smoke Hill Volcanics (e.g. GSWA 191706) and the 1068+\-7 Ma intrusive age of the Alcurra Dolerite (e.g. GSWA 194354). Forms scattered and poor outcrop in the core of Blackstone syncline (northern part of BLACKSTONE).|1073-1068 Ma|Unit of Tollu Group.||Upper unit of Tollu Group. Underlain conformably by Smoke Hill Volcanics.|Trachyandesite and trachydacite; basic to intermediate magmas interleaved with lenses of acicular- and comb-textured lavas, and basal interbedded volcaniclastic rocks, including pebble breccia and laminated volcanic siltstone, and lesser sandstone.|
8415|Hogarth Formation|68100|5|Briefly described|p5|||||Tollu Group|||Mafic Volcanics.|
8415|Hogarth Formation|68995|5|Briefly described|p8, p24, p29, p31, p34, p44 Fig.21, p45|Stenian|Stenian|Compositionally equivalent to the Alcurra Dolerite. Age is the crystallization age of a ferrogabbro in this unit. See also p51-52, p65.|1068 +/- 7 (GSWA 185518, Kirkland et al, 2013)|||Overlies the Smoke Hill Volcanics.|Basaltic andesite to dacite, trachyte and rhyolite.|
8415|Hogarth Formation|68996|5|Briefly described|p32-33, p43|Mesoproterozoic|Mesoproterozoic|||Tollu Group||Overlies Smoke Hill Volcanics.|Andesites with densities ranging from 2.69-2.76g/cm^3, Rhyolites with densities ranging from 2.61-2.98 g/cm^3.|17-JAN-17
8415|Hogarth Formation|69091|4|Described|p74, p144|Mesoproterozoic|Mesoproterozoic|Youngest rocks preserved in Blackstone Sub-basin (Figure 4.6). Compositionally identical to dolerites and ferrogabbros of Alcurra Dolerite and have an identical crystallisation age of 1068 +/- 7 Ma (GSWA 185518; Kirkland et al., in prep.).|1068 +/- 7 Ma, GSWA (2011)|Tollu Group||Overlies Smoke Hill Volcanics.||
8415|Hogarth Formation|69153|5|Briefly described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen||Tollu Group|||Andesitic to trachytic lavas; trachyandesite; dacite; felsic volcanic siltstone and sandstone; porphyritic rhyolite; felsic volcanic-pebble breccia; volcaniclastic rock fragments (matrix magnetite-rich rhyolite); metagabbro|
8415|Hogarth Formation|69436|5|Briefly described|p21:14|||Blackstone Sub-basin [Bentley Basin].||Tollu Group.||Is loosely correlated with Wankari Volcanics.||12-JUL-16
8415|Hogarth Formation|69729|5|Briefly described|p74 Fig.8, p80, p83|Mesoproterozoic|Mesoproterozoic|Rhyolite and basalt phases are shown as part of the Warakurna Supersuite. Trace element and age similarities with Alcurra Dolerite.|c.1068 Ma.|Tollu Group.||Conformably overlies Smoke Hill Volcanics.|Andesitic to rhyolitic rocks.|
8415|Hogarth Formation|70095|5|Briefly described|p16,18,21-22|||Geological province: Musgrave Province. Of Blackstone Sub-basin, Bentley Basin. Compositionally similar to Talbot rhyolites. Generally dacitic, with less depleted 18O magma. See p21 Table 3 for SIMS oxygen isotope data.||||||
8415|Hogarth Formation|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age from rhyolite sample (185518.1.pdf)|1026 Ma - 1073 Ma (Inferred) 1068 Ma  (SHRIMP)|Tollu Group||Overlies Smoke Hill Volcanics|Acicular and comb-textured andesitic to trachytic lavas, rare trachyandesite and dacite. Laminated felsic volcanic siltstone lesser sandstone and pebble breccia. Porphyritic rhyolite and lesser dacite; metagabbro.|
8415|Hogarth Formation|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 185518 (porphyritic rhyolite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1068+\-7 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv.|1073-1026 Ma (inferred)|||Uppermost unit of Tollu Group. Underlain by Smoke Hill Volcanics.|Andesitic to trachytic lavas, felsic volcanic pebble breccia, rhyolitic and dacitic volcanic and volcaniclastic fragments, laminated felsic volcanic siltstone and sandstone, metagabbro, porphyritic rhyolite and dacite.|
8415|Hogarth Formation|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Wankari Volcanics was established by Close et al., 2003a.|c. 1068 Ma|Tollu Group||Equivalent to the Wankari Volcanics.|Intermediate lavas.|
8415|Hogarth Formation|71211|5|Briefly described|p108 fig 3.11, p112, p233|||On the basis of geochemistry is interpreted to be an intermediate unit related to the Alcurra Dolerite Suite and the Rowland Suite.|ca. 1068 Ma|Tollu Group|||Dacites.|01-SEP-17
8415|Hogarth Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basic volcanic rock|
8415|Hogarth 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 185518 (rhyolite) yielded a concordia age of 1068+\-7 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 1m_geologyp12_lut.csv.|1073-1026 Ma (inferred)|Unit ofTollu Group.||Uppermost unit of Tollu Group. Underlain by Smoke Hill Volcanics.|Andesitic to trachytic lavas; rare trachyandesite and dacite; laminated felsic volcanic siltstone and lesser sandstone, porphyritic rhyolite and lesse dacite, felsic volcanic pebble breccia and metagabbro.|
8415|Hogarth Formation|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1068+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
8415|Hogarth Formation|72443|5|Briefly described|p743-748, p750, p753, p757|||Blackstone sub-basin of the Bentley Basin. Geochemistry is discussed. Compositionally very similar to the rocks of the Talbot Sub-basin.||Tollu Group||Overlies the Smoke Hill Volcanics.|Basaltic andesite to rhyolite.|
8432|Holmwood Shale|12758|5|Briefly described|p8 Fig. 9|Permian|Permian|Geological Province: Northern Perth Basin.||||||
8432|Holmwood Shale|14227|5|Briefly described|p7, p10|Permian|Early Carboniferous|Geological Province: Perth Basin. Glacio-marine sediments. See also Enclosure 2.||||||07-FEB-11
8432|Holmwood Shale|15881|5|Briefly described|p62|Permian|Permian|Contains Beckett and Fossil Cliff Members in the Irwin and Lockier River valley areas; and the Woolaga Limestone Member in the Woolaga Creek area. All members contains ammonoids.||||||12-FEB-09
8432|Holmwood Shale|22820|5|Briefly described|p10 Fig.4|Early Permian|Early Permian|Includes Beckett and Fossil Cliff Members.||||||12-AUG-08
8432|Holmwood Shale|23172|4|Described|Map Legend|Permian|Permian|||||||
8432|Holmwood Shale|23174|4|Described|Fig5p8,10|Early Permian|Late Carboniferous|||||||
8432|Holmwood Shale|23279|4|Described|p11-3,Fig2p3||Sakmarian|(Clarke et al., 1951).||||||
8432|Holmwood Shale|23520|5|Briefly described|p11 Fig. 7|Sakmarian|Sakmarian|Geological Province: Perth Basin.||||||
8432|Holmwood Shale|23761|5|Briefly described|p11|||||||||
8432|Holmwood Shale|23762|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||23-DEC-09
8432|Holmwood Shale|23816|4|Described|p231, 232|Sakmarian|Sakmarian|Geological Province: Perth Basin. Underlying unit: Nangetty Formation (conformable). Overlying unit: Fossil Cliff Formation (conformable). Max. thickness: 450 m. Contains the Beckett Member and Woolaga Limestone Member. Contains Juresanites jacksoni.||||||15-DEC-04
8432|Holmwood Shale|23935|6|Mentioned|p17|||Geological Province: Perth Basin.||||||22-FEB-05
8432|Holmwood Shale|24058|5|Briefly described|p111|Permian|Permian|Max. thickness: 555m. Geological Basin: Perth Basin.||||||22-JUL-09
8432|Holmwood Shale|24160|6|Mentioned|p94|||Northern Perth Basin.||||||
8432|Holmwood Shale|24443|5|Briefly described|Fig.30|Early Permian|Early Permian|Conformably overlies Nangetty Formation. Conformably overlain by High Cliff Sandstone. Geological Province: Bight Basin.||||||
8432|Holmwood Shale|29721|6|Mentioned|Table 226|||||||||
8432|Holmwood Shale|30263|6|Mentioned|Table 5|||Formation well bottomed in||||||
8432|Holmwood Shale|30545|6|Mentioned|Fig.2|||Sakmarian||||||
8432|Holmwood Shale|30948|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|30963|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|30973|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|31037|6|Mentioned|p1034|||Ammonoids external sutures. Sakmarian.||||||
8432|Holmwood Shale|31250|6|Mentioned|p7|||Microflora||||||
8432|Holmwood Shale|31251|6|Mentioned|p68|||Refers Crespin (1958)||||||
8432|Holmwood Shale|31394|6|Mentioned|p60|||See also P61,62. L.Permian||||||
8432|Holmwood Shale|31396|6|Mentioned|p1183|||||||||
8432|Holmwood Shale|31561|5|Briefly described|p5|||See also P18, 20, 24.||||||
8432|Holmwood Shale|31562|6|Mentioned|p10|||Stratigraphic Table||||||
8432|Holmwood Shale|31568|5|Briefly described|p19|||L. Permian||||||
8432|Holmwood Shale|31910|4|Described|Table 1|||P16||||||
8432|Holmwood Shale|32337|4|Described|p24|||||||||
8432|Holmwood Shale|32648|6|Mentioned|p32|||Sakmarian||||||
8432|Holmwood Shale|32649|4|Described|p17|||See also Table 1||||||
8432|Holmwood Shale|32714|6|Mentioned|Fig.2|||||||||
8432|Holmwood Shale|32840|6|Mentioned|Table 1|||||||||
8432|Holmwood Shale|32945|6|Mentioned|p87|||Permian. Correlated with Carrandibby Fm.||||||
8432|Holmwood Shale|33022|6|Mentioned|Fig.1|||||||||
8432|Holmwood Shale|33052|6|Mentioned|Fig.1|||Sakmarian||||||
8432|Holmwood Shale|33386|6|Mentioned|Fig.7|||||||||
8432|Holmwood Shale|33627|6|Mentioned|p582|||||||||
8432|Holmwood Shale|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
8432|Holmwood Shale|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
8432|Holmwood Shale|34532|6|Mentioned|Fig.2|||||||||
8432|Holmwood Shale|34841|6|Mentioned|Fig.2|||||||||
8432|Holmwood Shale|35268|6|Mentioned|p22|||||||||
8432|Holmwood Shale|35282|6|Mentioned|Fig.2|||See also Fig.26.||||||
8432|Holmwood Shale|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
8432|Holmwood Shale|35983|6|Mentioned|Table 26|||||||||
8432|Holmwood Shale|36020|6|Mentioned|p387|||||||||
8432|Holmwood Shale|36100|6|Mentioned|Fig.2|||||||||
8432|Holmwood Shale|36257|6|Mentioned|Table 2.1|||||||||
8432|Holmwood Shale|36265|5|Briefly described|Fig.3.26|Early Permian|Early Permian|Geological province: Perth Basin.||||||04-MAR-08
8432|Holmwood Shale|36293|2|Defined|p88|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|36718|6|Mentioned|p459|||||||||
8432|Holmwood Shale|36890|3|Fully described|p231|||||||||
8432|Holmwood Shale|36899|6|Mentioned|p1089|||||||||
8432|Holmwood Shale|37104|6|Mentioned|Fig.3|||||||||
8432|Holmwood Shale|37294|6|Mentioned|p100|||||||||
8432|Holmwood Shale|37298|6|Mentioned|Fig.1|||||||||
8432|Holmwood Shale|37549|6|Mentioned|Fig.4|||||||||
8432|Holmwood Shale|37812|6|Mentioned|p651|||||||||
8432|Holmwood Shale|37915|6|Mentioned|p459|||||||||
8432|Holmwood Shale|38217|5|Briefly described|p267|||Fossil correlations||||||
8432|Holmwood Shale|38444|6|Mentioned|p300|||||||||
8432|Holmwood Shale|38998|4|Described|p20|||See also P21.||||||
8432|Holmwood Shale|39263|6|Mentioned|p152|||||||||
8432|Holmwood Shale|40340|5|Briefly described|p13|||||||||
8432|Holmwood Shale|40341|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|40342|6|Mentioned|Map legend|Sakmarian|Sakmarian|||||||
8432|Holmwood Shale|40343|5|Briefly described|p10|||||||||
8432|Holmwood Shale|40346|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
8432|Holmwood Shale|40347|5|Briefly described|p23|||||||||
8432|Holmwood Shale|40992|6|Mentioned|Fig.5|||||||||
8432|Holmwood Shale|41044|6|Mentioned|p130|||||||||
8432|Holmwood Shale|41172|6|Mentioned|p121|||||||||
8432|Holmwood Shale|41192|6|Mentioned|Fig.5|||||||||
8432|Holmwood Shale|41195|6|Mentioned|Fig.2|||||||||
8432|Holmwood Shale|41315|6|Mentioned|p149|||||||||
8432|Holmwood Shale|41514|6|Mentioned|p62|||Includes 3 members: the Beckett and Fossil Cliff Members in the Irwin and Lockier River  Valleys; and the Woolaga Limestone Member in the Woolaga Creek area. All members contain ammonoids.||||||18-AUG-08
8432|Holmwood Shale|41728|6|Mentioned|p441|||||||||
8432|Holmwood Shale|41729|6|Mentioned|p453|||||||||
8432|Holmwood Shale|42017|6|Mentioned|p5|||||||||
8432|Holmwood Shale|42075|5|Briefly described|Fig.7 P247|||||||||
8432|Holmwood Shale|42309|6|Mentioned|p256|||||||||
8432|Holmwood Shale|42392|6|Mentioned|p115|||||||||
8432|Holmwood Shale|42473|6|Mentioned|p7|||||||||
8432|Holmwood Shale|42547|5|Briefly described|p105|||Permian.||||||
8432|Holmwood Shale|42687|6|Mentioned|map legend|||||||||
8432|Holmwood Shale|42688|6|Mentioned|map legend|||||||||
8432|Holmwood Shale|42711|6|Mentioned|p19|||Geological province: northern Perth Basin. Correlates with Moorhead Formation in the Collie Basin.||||||
8432|Holmwood Shale|42994|6|Mentioned|p36|||||||||
8432|Holmwood Shale|43015|5|Briefly described|Table 1,p319|||||||||
8432|Holmwood Shale|43018|5|Briefly described|Table 1,p386|||||||||
8432|Holmwood Shale|43031|4|Described|p11,Fig.2.|||||||||
8432|Holmwood Shale|43050|5|Briefly described|p7|||||||||
8432|Holmwood Shale|43067|5|Briefly described|p119|||see also Fig.12,p124||||||
8432|Holmwood Shale|43216|5|Briefly described|Map Legend||Permian|Perth Basin||||||
8432|Holmwood Shale|43217|5|Briefly described|Map Legend||Permian|Perth Basin||||||
8432|Holmwood Shale|43296|5|Briefly described|Map Legend||Permian|||||||
8432|Holmwood Shale|43297|4|Described|p4, fig.3 p5||Sakmarian|Also Table 1 p7.||||||
8432|Holmwood Shale|43347|6|Mentioned|13|||||||||
8432|Holmwood Shale|43495|4|Described|6-32||Sakmarian|||||||
8432|Holmwood Shale|43504|4|Described|4-9||Sakmarian|||||||
8432|Holmwood Shale|43882|14|Not recorded|p92|||Permian ammonoids.||||||
8432|Holmwood Shale|44144|4|Described|p508 Tb.4-21,p509 Fig.4-145,p510-3,p523|Sakmarian|Sakmarian|Type Section: Beckett Gully; 29o01'12''S 115o31'17''E. 450m thick shallow marine sediments; abundant shelly fauna in limestone Members. Sporadic glacial erratics indicate continued (post-Nangetty) presence of ice.|||Fossil Cliff, Beckett, Woolaga, Limestone Members.|Overlies Nangetty Formation gradationally. Overlain conformably by High Cliff Sandstone.|Grey-green shale and grey to black, well-bedded clayey siltstone; 3 fossiliferous limestone Members.|
8432|Holmwood Shale|44219|14|Not recorded|p31||Sakmarian|||||||
8432|Holmwood Shale|44237|14|Not recorded|p.200,203|||Fig. 2.||||||22-JUL-09
8432|Holmwood Shale|44378|14|Not recorded|p202||Sakmarian|Uraloceras irvinense.||||||
8432|Holmwood Shale|44994|6|Mentioned|Fig.7|||Permian. Correlation.||||||
8432|Holmwood Shale|44998|14|Not recorded|p.71||Sakmarian|||||||
8432|Holmwood Shale|45016|14|Not recorded|p.63|||Tb. at back. Correlated with Carrandibby Formation & Weedarra Shale.||||||
8432|Holmwood Shale|45104|6|Mentioned|p30|||||||||
8432|Holmwood Shale|46849|6|Mentioned|p186|||||||||
8432|Holmwood Shale|48615|14|Not recorded|p.11,13,14. Pl.2.|||(H50-1).||||||
8432|Holmwood Shale|48848|14|Not recorded|p.87,94,96,101|||||||||
8432|Holmwood Shale|49644|5|Briefly described|Table|||||||||
8432|Holmwood Shale|50107|5|Briefly described|Map legend|Permian|Permian|Geological Province: Northern Perth Basin.||||||
8432|Holmwood Shale|60295|5|Briefly described|p130|||Geological Province: Perth Basin||||||
8432|Holmwood Shale|60376|5|Briefly described|p17 Fig. 4.|Early Permian|Early Permian|Geological Province: Perth Basin. Overlain by High Cliff Sandstone. Underlain by Nangetty Formation.||||||07-FEB-11
8432|Holmwood Shale|60377|5|Briefly described|p61 Fig. 3, p64, p72|Sakmarian|Asselian|Overlain by High Cliff Sandstone. Underlain by Nangetty Formation. Geological Province: Perth Basin. Marine depositional Environment.||||||07-FEB-11
8432|Holmwood Shale|60386|5|Briefly described|p297, p309|Sakmarian|Sakmarian|Northern Perth Basin. Distal shelf/basin.|||||Fine-grained clastics.|
8432|Holmwood Shale|61546|6|Mentioned|p382, p385 Fig.5, p386. |Early Permian|Early Permian|Glacigene sediments.||||Overlies Nangetty Formation. Is overlain by High Cliff Sandstone.||
8432|Holmwood Shale|61811|4|Described|p3 Fig.2, pp36-45, p63.|Sakmarian|Asselian|Northern Perth Basin. Type section is along Beckett Gully 8 km south of Coalseam Conservation Park; further details in Appendix 1. 450 m thick.|||Includes Fossil Cliff, Woolaga Limestone and Beckett Members.|Conformably overlies Nangetty Formation. Is overlain by High Cliff Sandstone.|Glacigene deposits: grey-green shale and thin limestone beds, passing upwards into grey-black micaceous, jarositic, and gypsiferous shale and siltstone with minor discontinuous beds of fine-grained sandstone and coquinite; rare dropstones.|
8432|Holmwood Shale|62113|3|Fully described|pp618-621, pp625-628, p630.   |Sakmarian|Sakmarian|Maximum thickness of 700m. Well defined wave-influenced ripples with rare ice-rafted boulders, indicating cool but non-glacial conditions. Lower part resembles the Nangetty Formation: contains Sakmarian foraminifera and microfossils, and palynomorphs of ferns and lycopods, but upper parts have a paucity of ice-derived debris. |<290 Ma.||Includes the Fossil Cliff Member.|Overlies the Nangetty Formation. Is overlain unconformably by the High Cliff Sandstone.|Regressive succession of postglacial mudstone with bioclastic calcarenites and marine macrofossils. Laminated wave-influenced mudstones. Upper part bioclastic calcarenite beds.|
8432|Holmwood Shale|64580|4|Described|map legend||Early Permian|Grey shale, well-bedded clayey siltstone, interbedded limestone.||||||09-DEC-08
8432|Holmwood Shale|64630|5|Briefly described|p31 Fig.2, p33, 34|Sakmarian|Sakmarian|Province: Northern Perth Basin. Underlies the High Cliff Sandstone, overlies the Nangetty Formation. Palynology age: P. pseudoreticulata. Roughly correlates with Woodynook Sandstone. Glacial affinities uncertain.||||||24-NOV-09
8432|Holmwood Shale|64635|5|Briefly described|p4 Fig.3, p18-19, p21, p23-26       |Sakmarian|Sakmarian|Glacigene deposits ~450 m thick. Type section is along Beckett Gully 8 km south of Coalseam Conservation Park. Palynological and invertebrate faunal assemblages indicate a Sakmarian age (Segroves, 1971; Playford et al., 1976).|||Includes the Fossil Cliff, Woolaga Limestone, and Beckett, Members.|Overlies Nangetty Formation conformably. Is overlain by High Cliff Sandstone.|Comprises a section of grey-green shale and thin limestone beds in the lower part passing into grey-black micaceous, jarositic, and gypsiferous shale and siltstone with minor discontinuous sandstone and coquinite beds in the upper part.|
8432|Holmwood Shale|64972|6|Mentioned|p617 Fig. 4, p617 Fig. 5|Early Permian|Early Permian|Geological Province: Perth Basin.||||||
8432|Holmwood Shale|64974|5|Briefly described|p143, p144 Fig. 3|Sakmarian|Sakmarian|Includes Beckett and Woolaga Limestone Members. Geological Province: Perth Basin.||||||24-JUN-09
8432|Holmwood Shale|66949|6|Mentioned|p22|||Perth Basin.|||Includes Fossil Cliff Member.|||
8432|Holmwood Shale|67340|6|Mentioned|p6, 8, 25|Permian|Permian|Northern Perth Basin. Thermal rock properties.|||Fossil Cliff Member.|||
8432|Holmwood Shale|67354|6|Mentioned|p107.|||Perth Basin. Post-glacial unit, roughly contemporaneous with the Ditji Formation transgression in the Bonaparte Basin.||||||
8432|Holmwood Shale|67925|5|Briefly described|Ch4 p8 fig 2|Lower Permian|Lower Permian|Northern and central Perth Basin. ||||Overlies the Nangetty Formation. Overlain by the High Cliff Sandstone.||
8432|Holmwood Shale|69029|6|Mentioned|p332|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by Woodynook Sandstone. Underlain by Mosswood Formation.||
8432|Holmwood Shale|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p11, Ch2 p34-p41|Early Permian|Early Permian|Perth Basin. Is the oldest regional seal in the Perth Basin. See also  Ch2 p45, Ch2 p47-p49, Ch2 p55, Ch2 p57, Ch2 p60, Ch2 p64-p66, Ch2 p70, Ch2 p72, Ch2 p80, Ch2 p84, Ch2 p91, Ch2 p92, Ch2 p94-p96, Ch2 p98, Ch2 p100-p102, Ch2 p104, Ch2 p106, Ch2 p108, Ch2 p110.||||Overlies the Nangetty Formation. Overlain by the High Cliff Sandstone.|Glacial marine shales and silts with glacial debris.|
8432|Holmwood Shale|69547|4|Described|p180,182,188,193,196-199|Sakmarian|Sakmarian|northern Perth Basin. In the upper part of the Holmwood Shale type section, the limestone usually has a siliciclastic mud matrix and contains abundant bryozoan fragments, brachiopod debris, foraminifera, crinoid plates, ostracod valves, and gastropods. Depositional environment: more restricted marine conditions with large freshwater influx into the basin, bringing an abundant supply of mud derived from a previously glaciated landscape.|||Includes Fossil Cliff Member and Beckett Member.|Overlain by/prograded over by High Cliff Sandstone.|Marine mudstone.|
8432|Holmwood Shale|69583|5|Briefly described|p130, Plate 3.|Paleozoic|Paleozoic|Perth Basin.|||||Grey shale, well-bedded clayey siltstone, interbedded limestone.|
8432|Holmwood Shale|70097|5|Briefly described|p2, p20 Fig.4|Sakmarian|Sakmarian|Northern Perth Basin. Irwin Terrace, Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.||||Overlies Nangetty Formation. Is overlain by High Cliff Sandstone.|Pro-glacial marine basin fill. Includes shale.|12-SEP-17
8432|Holmwood Shale|70128|5|Briefly described|p449|Permian|Permian|Northern Perth Basin.||||Conformably overlies Nangetty Formation. Is overlain conformably by High Cliff Sandstone.||
8432|Holmwood Shale|70774|5|Briefly described|p5 fig 3|Sakmarian|Sakmarian|Northern Perth Basin.||||Overlies the Nangetty Formation. Overlain by the High Cliff Sandstone.||
8432|Holmwood Shale|70796|5|Briefly described|500k_interpgeop14_lut.csv|Sakmarian|Sakmarian|Perth Basin. Formed during Gondwana breakup along the western margin.|295  290.1 Ma (biostrat)||||Grey shale, wellbedded clayey siltstone, interbedded limestone|
8432|Holmwood Shale|71146|5|Briefly described|p6,  p43 fig 33|Sakmarian|Sakmarian|Perth Basin.||||Overlies the Nangetty Formation. Overlain by the High Cliff Sandstone.|Mudstone.|
8432|Holmwood Shale|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, limestone, shale|
8432|Holmwood Shale|71269|4|Described|GEOL_LUT_CSV files|Sakmarian|Sakmarian|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??.  See 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv.|292-290.1 Ma (biostrat)||||Grey shale, well-bedded clayey siltstone, interbedded limestone|
8432|Holmwood Shale|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Sakmarian|Perth Basin.  Age from biostratigraphy.||Permian package 1, Perth Basin.|||Grey shale, well-bedded clayey siltstone, interbedded limestone.|
8432|Holmwood Shale|72258|5|Briefly described|p129|Cisuralian|Cisuralian|Of Perth Basin.||||Overlain by High Cliff Sandstone. Underlain by Nangetty Formation. Laterally grades Woodynook Sandstone.||
8432|Holmwood Shale|72505|5|Briefly described|p890|Sakmarian|Asselian|Perth Basin. Correlated with the P.Confluens and Pseudoreticulosporta pseudoreticulata zones.||||Overlies the Nangetty Formation. Overlain by the High Cliff Sandstone.||
8432|Holmwood Shale|72910|6|Mentioned|p4 Fig.3.|Sakmarian|Sakmarian|Shown as part of the Northern Perth Basin.||||Overlies Nangetty Formation and underlies High Cliff Sandstone. Partially equivalent to Callytharra Formation and Lyons Group.||
8432|Holmwood Shale|73117|6|Mentioned|p15, p35|Asselian|Asselian|Includes the first appearance of Pseudoreticulatispora pseudoreticulata high in the unit.||||Underlain by Nangetty Formation. Overlain by High Cliff Sandstone.||
8432|Holmwood Shale|73484|5|Briefly described|p476 Fig.3|Cisuralian|Cisuralian|Perth Basin. Glaciogene.||||Overlies Nangetty Formation, underlies High Cliff Sandstone||
8432|Holmwood Shale|73513|4|Described|p30 Fig.2, p31-33, p35, p36 Fig.9|Sakmarian|Asselian|Perth Basin.||||Overlies Nangetty Formation, underlies High Cliff Sandstone with abrupt transition|Marine siltstone and shale, subordinate sandstone and limestone.|
8432|Holmwood Shale|73623|5|Briefly described|p1-6, 9-10, 12-17|Sakmarian|Sakmarian|Clarke et al. (1951). Irwin Basin. Thickness estimated at c.500m. Photographs, stratigraphic logs. Methane seeps are envisaged as centres (""oases"") of high marine organic productivity. Biota discussed in detail.|||Woolaga, Beckett, Limestone Members; Fossil Cliff Member.|Conformably overlies Nangetty Formation. Is overlain by High Cliff Sandstone. Correlative of Callytharra Formation.|Lacks diamictite; is highly friable. Contains localized nodular limestone deposits ("serpulid reefs") and cementstone nodules with preserved diverse and unusual fauna (discussed).|20-DEC-22
8438|Holstein Jaspilite Member|24165|5|Briefly described|p76|Archean|Archean|Iron King Mine, 5km SSE of Norseman. Mined for pyrite as a source of sulfur.||Noganyer Formation.||||
8438|Holstein Jaspilite Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
8438|Holstein Jaspilite Member|43162|6|Mentioned|6|||||||||
8463|Hong Kong Chert|30766|2|Defined|Appendix|Precambrian|Precambrian|||||||
8463|Hong Kong Chert|37373|6|Mentioned|p79|||||||||
8463|Hong Kong Chert|39697|6|Mentioned|p92|||||||||
8463|Hong Kong Chert|44150|6|Mentioned|p133 Tb.2-16|||West Pilbara. Of Fitton et al.(1975). Probably obsolete? Probably superseded by Towers Formation.||||||
8465|Honman Formation|22583|5|Briefly described|381|Archean|Archean|Geol province Yilgarn Craton. Max thickness 1200m. Overlying unit Glasse Formation, underlying unit Maggie Hays Formation||||||07-NOV-08
8465|Honman Formation|23129|5|Briefly described|p358|||Overlies Maggie Hays Formation.||||||
8465|Honman Formation|30969|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8465|Honman Formation|31093|2|Defined|p10|Archean|Archean|||||||07-NOV-08
8465|Honman Formation|65487|5|Briefly described|p5|||Part of the Lake Johnston Greenstone Belt, locally folded into the Burmister Syncline and the Gordon Anticline. Consists of metamorphosed BIF, clastic metasediments, metamorphosed ultramafics (including komatiite), and minor felsic metavolcanic and metavolcaniclastic rocks. Age 2921 +/- 4 Ma and 2903 +/- 5 Ma, from strata below and above the komatiite layer.||||||
8465|Honman Formation|68520|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. The 5 facies variants are mapped separately.|2930 - 2875 Ma (Mole et al 2012; Wang et al 1996)||||Chert and BIF; chert and BIF interleaved with komatiite; BIF and minor banded chert; dacitic volcanic and volcaniclastic rocks with subordinate rhyolite: all metamorphosed; felsic schist and interlayered psammitic and pelitic schist.|
8465|Honman Formation|69404|6|Mentioned|p8 Fig.9, p8|Mesoarchean|Mesoarchean|Lake Johnston greenstone belt, Southern Cross Domain. Less than 2km thick. Hosts the Maggie Hays nickel deposit. Maximum depositional age. |c. 2873 Ma (SHRIMP U-Pb, Thebaud et al., 2009)|||Overlies the Maggie Hays Formation, overlain by the Glasse Formation|Dacitic to rhyolitic volcanic to volcaniclastic rocks that are intruded by mafic-ultramafic rocks. At the top is a package of chemical sedimentary rocks with quartzite, chert and BIF.|
8465|Honman Formation|69559|4|Described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. One sub-unit (igneous felsic volcanic,A-_hm-xfd-fdv)  lists age range as 2856-2720 Ma. See also 100k_interpgeol_lut.csv, geologyp_lut.csv,  500k_interpgeol_lut.csv, 500k_interpgeop_lut.csv,  geologyl_lut.csv.|2873-2720 Ma||||Chert and banded iron formation, interleaved with komatiite. Felsic schist and interlayered psammitic and pelitic schists. Dacitic volcanic and volcaniclastic rocks with subordinate rhyolite.|
8465|Honman Formation|69617|5|Briefly described|p143, p145-155|||Gower and Bunting (1976). Lake Johnston greenstone belt, Youanmi Terrane, Yilgarn Craton. Recumbent folds, quartz veins and disruption from pegmatite veins and granitic gneiss. The Maggie Hays nickel deposit occurs in Roundtop Komatiite sills, below the meta-BIF unit. A volcaniclastic metasedimentary rock gave an age of c.2876 Ma (maximum deposition age).|2922 +/- 4 Ma and 2920 +/- 4 Ma (metavolcanics).|||Is overlain and intruded by Roundtop Komatiite.|Pale grey, metadacitic to metarhyolitic, metavolcanic and metavolcaniclastic rocks; overlain by quartzite, metachert and BIF, then garnetite and quartz-arenite.|
8465|Honman Formation|70144|5|Briefly described|Map legend|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. Geochronology by Mole et al. (2012) and Wang et al. (1996). The three facies are mapped separately.|2930-2720 Ma.||||Banded iron-formation and minor banded chert, metamorphosed; chert and banded iron-formation, metamorphosed; chert and banded iron-formation interleaved with komatiite, metamorphosed.|
8465|Honman Formation|70156|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010-2600 Ma); Youanmi Terrane events (3200-2600 Ma). See 500k_interpgeop14_lut.csv, 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 500k_interpgeol_lut.csv.|2930-2720 Ma (inferred)||||Chert, banded iron-formation, and siliciclastic sedimentary rock, interbedded with minor felsic volcanic rocks; metamorphosed|
8465|Honman Formation|70205|5|Briefly described|Map legend.|Archean|Archean|Southern Cross Domain, Youanmi Terrane, Yilgarn Craton. Five facies are mapped separately.|2930-2873 Ma.||||Chert, BIF and siliciclastic sedimentary rock, interbedded with minor felsic volcanic rock; metamorphosed (section only).|
8465|Honman Formation|70277|3|Fully described|p798-806,809-912|Mesoarchean|Mesoarchean|Geological province: Yilgarn Craton. Part of the ~2.9 Ga Lake Johnston greenstone belt, and contains a conformable basin stratigraphy that records the transition from felsic volcanism through exhalative iron formation to the intrusion and eruption of komatiitic magmas. U-Pb zircon ages of 2921+\-4 Ma and 2903+\-5 Ma (Wang et al., 1996). Comprises five laterally continuous lithologic units, from oldest to youngest. (1) The Felsic volcanic unit: at least 600m thick, with textures indicative of volcanism in subaqueous environment, derived from subduction and arc-related felsic volcanism. (2) the Transition zone unit: approx. 55m thick and marked by a basal garnet to garnet-amphibolite layer overlain by fine-grained massive silicious rocks with pyrrhotite stringers and fine disseminated sulfides, representing the cessation of felsic magmatism and onset of marine transgression. 3) The Banded iron formation unit: a homogeneous hydrothermal-sedimentary sequence of 120m average thickness, up to over 190m; representing a transition from low- to highstand conditions during a volcanic hiatus.  (4) the Sedimentary unit: representing subaerial protolith weathering and erosion and debris flow. (5) The Western ultramafic unit, comprising the eastern, central and western ultramafic units. The BIFs layer acted as a mechanical barrier to the underlying magma chamber (central ultramafic unit) before breaching and expulsion of komatiitic magmas across the basin floor.|||||(1)  Felsic volcaniclastics, feldspar- and quartz-porphyritic rocks (2) interbedded felsic volcanic rocks, sediments, and iron formation (3)  alternating magnetite and chert layers (4) quartz-arenite and massive sulfide (5) extrusive komatiites.|
8465|Honman Formation|70794|4|Described|100k_geologyp_lut.csv|Neoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Two age ranges shown in  500k_interpgeop14_lut.csv: 2930-2720 Ma and 2876-2730 Ma.See also 500k_interpgeop_lut.csv. |2920-2718 Ma inferred||||Chert, banded iron formation and siliciclastic sedimentary rock, interbedded with minor felsic volcanic rocks and komatiite. Metamorphosed. Chert and banded iron-formation interleaved with komatiite; metamorphosed.|
8465|Honman Formation|70802|5|Briefly described|500k_interpgeop14_lut.csv|Neoarchean|Mesoarchean|Geological province: Youanmi Terrane, Yilgarn Craton, West Australian Craton. Events: Youanmi Terrane events.|2930-2720 Ma (inferred)||||Chert, banded iron-formation, and siliciclastic sedimentary rock, interbedded with minor felsic volcanic rocks; metamorphosed|
8465|Honman Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Mesoarchean|Youanmi Terrane.|||Includes informal unnamed mameber.||Chert, banded iron-formation and siliciclastic sedimentary rocks; metamorphosed. Chert and banded iron-formation; metamorphosed.|
8465|Honman Formation|73596|6|Mentioned|p1170|Mesoarchean|Mesoarchean|Youanmi Terrane, Yilgarn Craton. Lake Johnston area.|2920 +/- 4 Ma.|Golden Grove Group.||||
8469|Hooper Complex|22526|6|Mentioned|Fig3 P682||Statherian|||||||
8469|Hooper Complex|22547|6|Mentioned|p8||Siderian|King Leopold Orogen. Maximum age 2500 Ma.||||||14-NOV-06
8469|Hooper Complex|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|||||||
8469|Hooper Complex|22754|5|Briefly described|p2 Fig. 1|||||||||
8469|Hooper Complex|23383|6|Mentioned|p8,  p4 Fig. 2|||See also mention on p21.||||||25-JAN-05
8469|Hooper Complex|23599|5|Briefly described|p4 Fig 2|||||||||
8469|Hooper Complex|23722|4|Described|p5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8469|Hooper Complex|23751|6|Mentioned|p4|||||||||
8469|Hooper Complex|24197|6|Mentioned|p23|||Superseded and incorporated into the Paperbark Supersuite.||||||07-FEB-11
8469|Hooper Complex|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8469|Hooper Complex|42778|5|Briefly described|p13|||Variation on Hooper West lamproite?||||||
8469|Hooper Complex|42811|4|Described|p3|||||||||
8469|Hooper Complex|42814|4|Described|p5|||||||||
8469|Hooper Complex|44140|6|Mentioned|p293; p296-298 figs.4-4,-5; p300; p304|||The Kimberley Basin succession has been thrust from the NE over the Hooper Complex.||||Is overlain unconformably by, and thrust-faulted under, the Speewah Group.||07-MAR-18
8469|Hooper Complex|44155|4|Described|p232-255|Paleoproterozoic|Paleoproterozoic||||Includes Kongorow Granite and Nellie Tonalite.|||
8469|Hooper Complex|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Metamorphic rocks and granites.||||||07-NOV-08
8469|Hooper Complex|50437|6|Mentioned|p2.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite. Age: 1860Ma.||||||07-NOV-08
8469|Hooper Complex|50543|5|Briefly described|Map|||Structural term in this context.||||||
8469|Hooper Complex|60714|6|Mentioned|p113 Fig.2. |Orosirian|Orosirian|Part of basement to Speewah Basin.|1890-1840 Ma.|||||
8469|Hooper Complex|60724|6|Mentioned|p3 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8469|Hooper Complex|61564|6|Mentioned|p589 Fig. 1|||Structural term in this context.||||||
8469|Hooper Complex|61571|5|Briefly described|p654 Fig. 1|Paleoproterozoic|Paleoproterozoic|Together with the Lamboo Complex forms the Palaeoproterozoic crystalline basement of the Kimberley Basin.||||||07-NOV-08
8469|Hooper Complex|62715|6|Mentioned|p1753, p1779|||Within the Halls Creek and King Leopold Orogens.||||||04-OCT-06
8469|Hooper Complex|63869|6|Mentioned|p3 Fig.1|||||||||
8469|Hooper Complex|64104|6|Mentioned|p76 fig 10|||||||||
8469|Hooper Complex|64635|6|Mentioned|p2 Fig.1|||||||||
8469|Hooper Complex|64731|5|Briefly described|p164|Paleoproterozoic|Paleoproterozoic|Geological Province or unit name? Dated at 1860-1850 Ma, of Halls Creek Orogen.||||||12-APR-12
8469|Hooper Complex|64748|6|Mentioned|p269 Fig 2|Orosirian|Orosirian|Shown as 1890 - 1840 Ma||||||
8469|Hooper Complex|66845|5|Briefly described|p535, p536, p540, p543|Paleoproterozoic|Paleoproterozoic|Tyler et al. (1995, 1999) concluded that the Western zone of Lamboo Complex (Halls Creek Orogen) is a continuation of the Hooper Complex (King Leopold Orogen).||||||
8469|Hooper Complex|67323|5|Briefly described|p29|||Tyler et al. (1999). Turbidites deposited onto the Kimberley Craton. Shown as Hooper Complex (Lamboo Complex).|~1870-1865 Ma.|||||
8469|Hooper Complex|67563|6|Mentioned|p121, p122 Fig.2, p123|||||||||
8469|Hooper Complex|68992|5|Briefly described|p498 Fig.1, p499|Orosirian|Orosirian||1890-1840 Ma|||Unconformably overlain by the Speewah Group. Intruded by the Hart Dolerite.|Comprises siliciclastic rocks.|
8469|Hooper Complex|69099|5|Briefly described|geochron file 182107.1.pdf|Paleoproterozoic|Paleoproterozoic|See geochron file 182107.1.pdf for unit relationships.|1865-1850 Ma|||Unconformably overlain by O'Donnell Formation, Speewah Group.||
8469|Hooper Complex|73184|6|Mentioned|p192|||Kimberley region, contains detrital zircons ages less than 2.55 Ga (Tyler et al., 1999).||||||
8470|Hooper West lamproite|41158|6|Mentioned|p156|||||||||
8485|Hopetoun Jaspilite Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
8485|Hopetoun Jaspilite Member|43162|6|Mentioned|6|||||||||
8488|Horan's Line gabbro|41249|5|Briefly described|p23|||||||||
8493|Horn Valley Siltstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Siltstone, fossiliferous limestone, minor thin sandstone.||||||
8493|Horn Valley Siltstone|12891|5|Briefly described|p733 Fig. 2|Early Ordovician|Early Ordovician|Geological province: Amadeus Basin.||||||07-FEB-11
8493|Horn Valley Siltstone|13995|5|Briefly described|p73, p79-80, p83, p87, p89, p99-102|Middle Ordovician|Middle Ordovician|Amadeus Basin. Brachiopod species. Relatively small number of nautiloids. Graptolites mentioned. Conodonts in this unit also occur in Argentina. Contains microvertebrate remains. Biogeographic links discussed.||||Is overlain conformably by Stairway Sandstone.||
8493|Horn Valley Siltstone|22560|5|Briefly described|p3|||||||||
8493|Horn Valley Siltstone|22561|4|Described|p28|Neoproterozoic|Neoproterozoic|Also see Horn Valley Formation p9. Pacoota Sandstone underlies Horn Valley Siltstone.||||||06-FEB-08
8493|Horn Valley Siltstone|22565|6|Mentioned|p71 in Table 1|||Thickness at Areyonga Creek measured from surface expression 110m thick.  Approx. thickness measured from seismic data - 130m.||||||
8493|Horn Valley Siltstone|22566|5|Briefly described|p85|Early Ordovician|Early Ordovician|Of the Larapinta Group.||||||26-SEP-06
8493|Horn Valley Siltstone|22646|5|Briefly described|p104|Arenig|Arenig|Age - early Arenig to middle Arenig   (Ordovician)||||||26-SEP-06
8493|Horn Valley Siltstone|22650|4|Described|p 160|Ordovician|Ordovician|Of the Larapinta Group.||||||26-SEP-06
8493|Horn Valley Siltstone|22651|6|Mentioned|Fig 10 btw p182-183|Ordovician|Ordovician|||||||
8493|Horn Valley Siltstone|22655|5|Briefly described|p 272|||||||||
8493|Horn Valley Siltstone|22656|4|Described|p 278|Early Ordovician|Early Ordovician|||||||
8493|Horn Valley Siltstone|22758|5|Briefly described|p307|||Informally devided into upper and lower Horn Valley Siltstone.  Age - Mid to early Arenig.||||||
8493|Horn Valley Siltstone|22759|4|Described|p317-319|Early Ordovician|Early Ordovician|Age - Arenig.  Unit sub-devided into ten informal members, HV1 (lower most) to HV10, which reflect vertical lithofacies variations in a shallow marine shelf environment.||||||
8493|Horn Valley Siltstone|22760|5|Briefly described|p344|||||||||
8493|Horn Valley Siltstone|22763|6|Mentioned|table 1 on p386||Early Ordovician|Parent - Larapinta Group.||||||
8493|Horn Valley Siltstone|22804|6|Mentioned|Fig 2 on p432|||Parent - Larapinta Group.  Age - ?Ordovician.||||||
8493|Horn Valley Siltstone|22805|4|Described|p471|Early Ordovician|Early Ordovician|The Horn Valley Siltstone acts as a source for the Stairway Sandstone and as both a source and seal for the Pacoota Sandstone.||||||
8493|Horn Valley Siltstone|22806|4|Described|p485|Ordovician|Ordovician|||||||
8493|Horn Valley Siltstone|22807|4|Described|p506|Early Ordovician|Early Ordovician|Of the Larapinta Group.||||||26-SEP-06
8493|Horn Valley Siltstone|22823|4|Described|p514- 517||Ordovician|||||||
8493|Horn Valley Siltstone|22825|6|Mentioned|p553|||||||||
8493|Horn Valley Siltstone|22826|5|Briefly described|p572|Ordovician|Ordovician|Of the Larapinta Group.||||||26-SEP-06
8493|Horn Valley Siltstone|23282|6|Mentioned|p82|||Probably equivalent to Indulkana Shale. of Amadeus Basin.||||||
8493|Horn Valley Siltstone|23361|5|Briefly described|16 Fig.4|Cambrian|Cambrian|||||||
8493|Horn Valley Siltstone|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|29721|6|Mentioned|Table 44|||||||||
8493|Horn Valley Siltstone|29972|6|Mentioned|Table 1|||Lower Ordovician||||||
8493|Horn Valley Siltstone|30238|4|Described|p68|||Cambrian - Ordovician||||||
8493|Horn Valley Siltstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group.||||||
8493|Horn Valley Siltstone|30540|6|Mentioned|p61|||Main source rock for Mereenie & Palm Valley Fields||||||
8493|Horn Valley Siltstone|30544|6|Mentioned|p49|||||||||
8493|Horn Valley Siltstone|30615|6|Mentioned|p177|||Stratigraphic table Palm Valley -2||||||
8493|Horn Valley Siltstone|31572|6|Mentioned|p22|||||||||
8493|Horn Valley Siltstone|31707|4|Described|p53|||Lithology||||||
8493|Horn Valley Siltstone|32854|6|Mentioned|p352|||||||||
8493|Horn Valley Siltstone|33307|6|Mentioned|Fig.6|||L.Ord.||||||
8493|Horn Valley Siltstone|33738|6|Mentioned|p47|||||||||
8493|Horn Valley Siltstone|33761|6|Mentioned|p146|||Ordovician||||||
8493|Horn Valley Siltstone|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also p8.||||||26-SEP-06
8493|Horn Valley Siltstone|34280|6|Mentioned|p10|||||||||
8493|Horn Valley Siltstone|34401|5|Briefly described|p70|||||||||
8493|Horn Valley Siltstone|34442|5|Briefly described|Table 1|||Cambrian to Ordovician.||||||
8493|Horn Valley Siltstone|35102|6|Mentioned|Fig.2|||||||||
8493|Horn Valley Siltstone|35628|6|Mentioned|p4|||||||||
8493|Horn Valley Siltstone|36047|6|Mentioned|p369|||||||||
8493|Horn Valley Siltstone|36096|6|Mentioned|p219|||||||||
8493|Horn Valley Siltstone|36128|6|Mentioned|p13|||||||||
8493|Horn Valley Siltstone|36198|6|Mentioned|Fig.III.2|||||||||
8493|Horn Valley Siltstone|36818|6|Mentioned|p203|||||||||
8493|Horn Valley Siltstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
8493|Horn Valley Siltstone|40136|5|Briefly described|p27|||||||||
8493|Horn Valley Siltstone|40137|6|Mentioned|Table 1|||||||||
8493|Horn Valley Siltstone|40740|3|Fully described|p52|||Mention p6.||||||26-SEP-06
8493|Horn Valley Siltstone|40810|4|Described|p9|||||||||
8493|Horn Valley Siltstone|40830|6|Mentioned|p12|||||||||
8493|Horn Valley Siltstone|41039|4|Described|p6|||||||||
8493|Horn Valley Siltstone|41115|6|Mentioned|Fig.2|||||||||
8493|Horn Valley Siltstone|41190|5|Briefly described|p267|||||||||
8493|Horn Valley Siltstone|41203|5|Briefly described|p60|||Mention p5.||||||26-SEP-06
8493|Horn Valley Siltstone|41224|6|Mentioned|p430|||||||||
8493|Horn Valley Siltstone|41270|6|Mentioned|p274|||||||||
8493|Horn Valley Siltstone|41385|6|Mentioned|Fig.2|||||||||
8493|Horn Valley Siltstone|41621|5|Briefly described|Map legend|Ordovician||||||||
8493|Horn Valley Siltstone|41639|6|Mentioned|p17|||||||||
8493|Horn Valley Siltstone|41708|6|Mentioned|p206|||||||||
8493|Horn Valley Siltstone|41723|6|Mentioned|Map legend|Ordovician||||||||
8493|Horn Valley Siltstone|41819|6|Mentioned|Map legend|Ordovician||||||||
8493|Horn Valley Siltstone|41820|4|Described|p10|||||||||
8493|Horn Valley Siltstone|42037|5|Briefly described|Table 3 P79|||||||||
8493|Horn Valley Siltstone|42049|6|Mentioned|p220|||||||||
8493|Horn Valley Siltstone|42058|6|Mentioned|p123|||||||||
8493|Horn Valley Siltstone|42059|5|Briefly described|Fig.2 P131|||||||||
8493|Horn Valley Siltstone|42060|6|Mentioned|Fig.5 P140|||||||||
8493|Horn Valley Siltstone|42082|4|Described|p322|||||||||
8493|Horn Valley Siltstone|42354|4|Described|Fig.3 P5, P6|||||||||
8493|Horn Valley Siltstone|42504|6|Mentioned|p77|||||||||
8493|Horn Valley Siltstone|42940|5|Briefly described|Plate 8|||||||||
8493|Horn Valley Siltstone|43035|6|Mentioned|p38|||||||||
8493|Horn Valley Siltstone|43105|5|Briefly described|p8|||||||||
8493|Horn Valley Siltstone|43117|5|Briefly described|Table 1,p349|||||||||
8493|Horn Valley Siltstone|43225|5|Briefly described|Map Legend||Ordovician|Of Larapinta Group||||||26-SEP-06
8493|Horn Valley Siltstone|43230|6|Mentioned|p9||Ordovician|Source rock.||||||
8493|Horn Valley Siltstone|43503|6|Mentioned|11-50|Yapeenian|Bendigonian|||||||
8493|Horn Valley Siltstone|43646|6|Mentioned|p553||Early Ordovician|||||||
8493|Horn Valley Siltstone|43648|6|Mentioned|p491|||||||||
8493|Horn Valley Siltstone|43649|5|Briefly described|p457|||||||||
8493|Horn Valley Siltstone|43803|6|Mentioned|Fig.5,p71|||||||||
8493|Horn Valley Siltstone|43808|6|Mentioned|p297|||||||||
8493|Horn Valley Siltstone|43809|6|Mentioned|p213||Early Ordovician|||||||
8493|Horn Valley Siltstone|43869|5|Briefly described|p10||Cambrian|Mud-rich sedimentary rock containing an abundance of fossils; rich petroleum source.  Overlies Pacoota Sandstone.||||||12-SEP-05
8493|Horn Valley Siltstone|44133|6|Mentioned|p41|||Correlated to Indulkana Shale. ||||||
8493|Horn Valley Siltstone|44395|14|Not recorded|p.8, Tb.2||Early Ordovician|Lower Ordovician.||||||
8493|Horn Valley Siltstone|44396|5|Briefly described|map legend|||(Camb-Ord). Of Larapinta Group. SF/52-15.||||||26-SEP-06
8493|Horn Valley Siltstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
8493|Horn Valley Siltstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
8493|Horn Valley Siltstone|44484|14|Not recorded|p.11,12,13, Tb.1|Ordovician|Cambrian|||||||
8493|Horn Valley Siltstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
8493|Horn Valley Siltstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Camb-Ord.||||||
8493|Horn Valley Siltstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
8493|Horn Valley Siltstone|44505|14|Not recorded|p.3,8,11,12, Table 1|||Of Larapinta Group (Camb-Ord).||||||
8493|Horn Valley Siltstone|44506|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
8493|Horn Valley Siltstone|45036|6|Mentioned|p3|||Lower Ordovician||||||
8493|Horn Valley Siltstone|45041|4|Described|p68|||See also pp69-71. L.Ord.||||||26-SEP-06
8493|Horn Valley Siltstone|45115|6|Mentioned|p5|||||||||
8493|Horn Valley Siltstone|45118|6|Mentioned|p3|||||||||
8493|Horn Valley Siltstone|45148|6|Mentioned|Fig.4|||Amadeus Basin||||||
8493|Horn Valley Siltstone|45155|6|Mentioned|Fig.8|||||||||
8493|Horn Valley Siltstone|45170|6|Mentioned|p23|||||||||
8493|Horn Valley Siltstone|46928|6|Mentioned|Table 1|||||||||
8493|Horn Valley Siltstone|47052|6|Mentioned|p261|||||||||
8493|Horn Valley Siltstone|48639|14|Not recorded|p.7|||Missing in section in Alice No.1.||||||
8493|Horn Valley Siltstone|48862|14|Not recorded|p.8-27,42,43;Pl.9-11||Early Ordovician|Name supersedes 'Horn Valley Fm'. L.Ord. (F52-15).||||||
8493|Horn Valley Siltstone|48863|2|Defined|p.26|||Tb.1. oppp.7, p.9,19,20,24,28-30,40,41,Pl.9,11,13-15-16. (G52-4,G53-1).||||||
8493|Horn Valley Siltstone|48864|14|Not recorded|p.10(Tb),32.||Ordovician|||||||
8493|Horn Valley Siltstone|48865|14|Not recorded|Fig.4,opp.p.10,p.23|||(F53-13,G52-4).||||||
8493|Horn Valley Siltstone|48890|4|Described|p.45||Ordovician|Of the Larapinta Gp.||||||26-SEP-06
8493|Horn Valley Siltstone|48963|6|Mentioned|p5|||||||||
8493|Horn Valley Siltstone|50089|5|Briefly described|p427, p429 Fig. 3|Ordovician|Ordovician|Oepikodus cleftus (conodont) found in this siltstone. Geological Province: Canning Basin.||||||
8493|Horn Valley Siltstone|50098|5|Briefly described|p1|Early Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Green lamintaed siltstone with fine sandstone interbeds, fossiliferous limestone. Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
8493|Horn Valley Siltstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, shale, limestone; marine fossils.   Geological Province: Ngalia Basin [?check map]||||||20-OCT-10
8493|Horn Valley Siltstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Siltstone, shale, limestone; marine fossils. Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Green laminated siltstone with fine grained sandstone interbeds, fossiliferous limestone. Geological Province: Amadeus Basin.||||||
8493|Horn Valley Siltstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Siltstone, shale, limestone; marine limestone. Geological Province: Amadeus Basin.||||||14-FEB-06
8493|Horn Valley Siltstone|61551|5|Briefly described|p352.|Arenigian|Arenigian|Amadeus Basin. Hydrocarbon source rock.|485-470 Ma.|||||
8493|Horn Valley Siltstone|62359|5|Briefly described|p542, p546|||Overlies Pacoota Sandstone. Forms the seal for reservoir in underlying sandstone. Geological Province: Amadeus Basin. See also p546-547 Figs. 6 and 7.||||||
8493|Horn Valley Siltstone|62376|5|Briefly described|p18|Early Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
8493|Horn Valley Siltstone|62379|4|Described|p7 Fig. 2, p10|Ordovician|Ordovician|Of the Larapinta Group. Geol. Prov: Amadeus Basin. Age: 472-468Ma. Overlies: Pacoota Sst and underlies Stairway Sst. Thinly interbedded sltst and shale, minor lst. Max. thick: 120m.||||||
8493|Horn Valley Siltstone|62794|3|Fully described|p288, p289-299|Early Ordovician|Early Ordovician|Unit in Larapinta Group, unconformably overlying Pacoota Sandstone and unconformably underlying Stairway Sandstone in Waterhouse Range area . Type section at Ellery Creek. Boundaries discussed. Poorly outcropping siltstones, limestones, minor sandstone. Highly fossiliferous.||||||22-JAN-13
8493|Horn Valley Siltstone|62795|6|Mentioned|p348|Early Ordovician|Early Ordovician|Amadeus Basin. Fossiliferous. Contains similar trilobite fauna  to part of Rowena Formation.||||||
8493|Horn Valley Siltstone|62982|5|Briefly described|p7|Early Ordovician|Early Ordovician|Of the Larapinta Group. Marine deposits. Overlies Pacoota Sandstone; overlain by Stairway Sandstone. Geological Province: Amadeus Basin. Main source unit for oil and gas fields of the Larapinta group.||||||16-JAN-07
8493|Horn Valley Siltstone|63562|6|Mentioned|p338 fig 3, p352 fig 10|Early Ordovician|Early Ordovician|Of Amadeus Basin.||Larapinta Group.||Overlies Pacoota Sandstone. Is overlain by Stairway Sandstone.||
8493|Horn Valley Siltstone|64015|5|Briefly described|p67|Early Ordovician|Early ordovician|Geological province: Amadeus Basin.||||||28-AUG-08
8493|Horn Valley Siltstone|64068|6|Mentioned|p76, 77, 226|||Amadeus Basin.  Correlated with Coolibah Formation, in part with Nora Formation, Georgina Basin.||||||
8493|Horn Valley Siltstone|64334|5|Briefly described|p39-43|Ordovician|Ordovician|Amadeus Basin. Gas and oil source rock; also acts as a seal.||Larapinta Group.||Overlies Pacoota Sandstone. Is overlain unconformably by Stairway Sandstone.|Chemically-reduced and in part organic-rich mudstone, fine sandstone with thin carbonate interbeds. Richly fossiliferous.|
8493|Horn Valley Siltstone|64778|6|Mentioned|p13, 18, 21, 26-28|Ordovician|Ordovician|Amadeus Basin. Potential hydrocarbon source rock. Appears as HVS in much of the text.||||Is overlain by Stairway Sandstone.||
8493|Horn Valley Siltstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10. |Early Ordovician|Early Ordovician|See also p13 Fig.13. Deposition on an open shelf in well-oxygenated waters.||Of the Larapinta Group|||Euxinic marl, mud and silt; richly fossiliferous.|
8493|Horn Valley Siltstone|64982|6|Mentioned|p705.|||Amadeus Basin. Has distinctive signature of oils derived from G. prisca-rich source; closely matches oils from Looma 1 well.||||||
8493|Horn Valley Siltstone|65233|3|Fully described|p3 Fig. 2, p10|Early Ordovician|Early Ordovician|Of lower Larapinta Group. Gradational with Pacoota Sst below and with overlying Stairway Sst. Max. thickness: 120m. Geological province: Amadeus Basin. Contains the most important oil/gas source rocks in the Amadeus Basin. Lithological details included.||||||07-FEB-11
8493|Horn Valley Siltstone|65239|5|Briefly described|p2|Ordovician|Ordovician|Geological province: Amadeus Basin. Hosts important petroleum system.||||||04-JUN-09
8493|Horn Valley Siltstone|65313|5|Briefly described|p578, p579|Middle Ordovican|Middle Ordovican|Amadeus Basin. Castlemanian trilobite assemblage (Lycophron freemani).||||||26-MAR-12
8493|Horn Valley Siltstone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 60 m.||||Overlies Pacoota Sandstone. Is overlain by Stairway Sandstone.||
8493|Horn Valley Siltstone|65489|5|Briefly described|p56, p125|Ordovician|Ordovician|Amadeus Basin.||Unit in Larapinta Group.||Overlies Pacoota Sandstone. Is overlain by Stairway Sandstone.||
8493|Horn Valley Siltstone|66623|6|Mentioned|p157.|||Amadeus Basin. Age-correlative with Tabita Formation, Pimbilla Tank Group.||||||
8493|Horn Valley Siltstone|66767|5|Briefly described|p60|Ordovician|Ordovician|NE Amadeus Basin. The most important petroleum source rock in the Basin.||Larapinta Group.||||
8493|Horn Valley Siltstone|67126|5|Briefly described|p1-8, p10-13, p21, p27-28, p33, p36-38|Early Ordovician|Early Ordovician|Amadeus Basin. Might have gas shale potential (reasons detailed). Rock Eval analysis, Rock Eval Temperature Programme: Pyrolysis, Thermovaporisation, Pyrolysis Gas Chromatography results presented in detail.||||||
8493|Horn Valley Siltstone|67326|5|Briefly described|p2-4|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Pacoota Sandstone. Is overlain by Stairway Sandstone.||
8493|Horn Valley Siltstone|67565|5|Briefly described|p41, p51.|Middle Ordovician|Early Ordovician|A recessive unit, mainly outcropping on valley floors. An important petroleum source rock with a high organic content; also forms the caprock to the Pacoota Sandstone oil and gas reservoir. Thickness to 429 m. Richly fossiliferous.||||Conformably overlies Pacoota Sandstone.|Green laminated siltstone with fine-grained grey-green sandstone interbeds, overlain by siltstone with interbeds of blue-grey and yellow-brown fossiliferous limestone.|
8493|Horn Valley Siltstone|67856|6|Mentioned|p338 fig 4-30|Early Ordovician|Early Ordovician|||Of Larapinta Group.||||
8493|Horn Valley Siltstone|68297|5|Briefly described|p177|Bendigonian|Bendigonian|Amadeus Basin. Includes disarticulated vertebrate fossils. ||||||
8493|Horn Valley Siltstone|68323|6|Mentioned|p4 Fig.2|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
8493|Horn Valley Siltstone|69206|6|Mentioned|p2|Ordovician|Ordovician|Amadeus Basin. Source of the Mereenie oil.||||||
8493|Horn Valley Siltstone|69418|5|Briefly described|p3:36|Ordovician|Ordovician|Amadeus Basin. Hosts the Mereenie (oil and gas) and the Palm Valley (gas) fields. Has unconventonal petroleum potential (shale gas and oil).||||||12-JUL-16
8493|Horn Valley Siltstone|69437|5|Briefly described|p22:10, 15-16|Ordovician|Ordovician|Amadeus Basin. Has considerable unconventional petroleum potential: shale gas and oil.||||Overlies Pacoota Sandstone. Is overlain by Stairway Sandstone.||12-JUL-16
8493|Horn Valley Siltstone|69438|2|Defined|p23:2-3, 7, 33-34, 54-61|Middle Ordovician|Early Ordovician|Wells et al. (1965). Originally the Horn Valley beds (Madigan, 1932) with a type section at Ellery Creek. Subsequently renamed Horn Valley Formation by Pritchard and Quinlan (1965). Rocks (palaeontological descriptions) first described by Tate (1896). Amadeus Basin. Generally poorly exposed. The base is defined as the first prominent limestone bed above the siliciclastic Pacoota Sandstone. Thickens northwards up to c.442m. Characterised by abundant and well-preserved faunal and floral assemblages (listed). The source rock, and regional seal, for hydrocarbon reservoirs at Mereenie and Palm Valley petroleum fields; also has significant potential for shale gas. Contains oolitic ironstone beds with little economic significance. This unit is the hydrocarbon source rock for the production fields at Mereenie and Palm Valley; described in some detail. Thick shales seal Pacoota Sandstone reservoirs. Has good shale gas potential.||Larapinta Group.||Overlies Pacoota Sandstone probably unconformably. Is overlain unconformably by Stairway Sandstone.|Thinly bedded shale and siltstone, with bedded nodular limestone abundant in some intervals. The shale is organic-rich in the subsurface,  and limestone is subordinate, with interbeds of sandy phosphatic and glauconitic layers.|12-JUL-16
8493|Horn Valley Siltstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
8493|Horn Valley Siltstone|69447|6|Mentioned|p32:10|Ordovician|Ordovician|Amadeus Basin. Prolific petroleum system.||||||12-JUL-16
8493|Horn Valley Siltstone|69449|6|Mentioned|p34:2 Fig.34.2|Ordovician|Ordovician|Eastern Amadeus Basin.||||||12-JUL-16
8493|Horn Valley Siltstone|69673|5|Briefly described|p66, p78, p80, p90, p92, p99, p136, |Ordovician|Cambrian |Approximately 422m thick. Primary source rock in the lower Larapinta Group (only commercially productive petroleum system in the basin)||Larapinta Group||conformably overlies Pacoota Sandstone, disconformably overlain by Stairway Sandstone|Organic rich shale and siltstone with bedded nodular limestone.|
8493|Horn Valley Siltstone|70061|6|Mentioned|Regional geology p8|||Amadeus Basin. Oil-prone.||||||12-JUL-16
8493|Horn Valley Siltstone|71146|5|Briefly described|p6, p43 fig 33|Middle Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group||Overlies the Pacoota Sandstone. Unconformably overlain by the Stairway Sandstone.|Carbonate, mudstone and siltstone.|
8493|Horn Valley Siltstone|71171|6|Mentioned|p2|||Amadeus Basin.||||||
8493|Horn Valley Siltstone|71279|5|Briefly described|p355 Fig.2, p365, p374|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
8493|Horn Valley Siltstone|71800|6|Mentioned|p26 fig 3|Middle Ordovician|Middle Ordovician|Amadeus Basin.||||Overlies the Pacoota Sandstone. Unconformably overlain by the Stairway Sandstone.||
8493|Horn Valley Siltstone|71898|4|Described|iii, p1, p3, p20-p22|Middle Ordovician|Early Ordovician|Amadeus Basin. Originally described by Pritchard and Quinlan (1962) as being conformable on the Pacoota Sandstone; however, Gorter (1991) demonstrated an unconformable contact in several areas. Outcrops on the PALM VALLEY Sheet (5440) in strike valleys with the best exposures in the MacDonnell Ranges and on the flanks of some anticlines west of Tempe Downs homestead. SHRIMP age is interpreted to be a maximum depositional age and correlates well with an early to middle Ordovician age derived from faunal and floral fossil assemblage. Sample location, description at location, zircon morphology, SHRIMP analysis, results and methods are discussed. This unit has an estimated maximum thickness of 422m.|487 +/- 12 Ma (SHRIMP U-Pb)|Larapinta Group||Overlies the Pertaoorrta Group. Unconformably overlain by the Stairway Sandstone.|Thinly-bedded shale and siltstone with bedded nodular limestone abundant in some intervals.|
8493|Horn Valley Siltstone|72360|5|Briefly described|Map legend|Ordovician|Ordovician|Of Amadeus Basin.||Unit of Larapinta Group.|||Siltstone, shale, limestone; marine fossils.|09-SEP-19
8493|Horn Valley Siltstone|72369|5|Briefly described|p26,34|||Of Amadeus Basin.||Unit of Larapinta Group.||Overlain disconformably by Stairway Sandstone. Underlain by Pacoota Sandstone.||
8493|Horn Valley Siltstone|73085|4|Described|piii, p1, p3-8, p11|early Ordovician|early Ordovician|Amadeus Basin. 15 m thick in drillhole LA05DD01. Basal contact with Pacoota Sandstone is transitional.||Larapinta Group||Underlain by Pacoota Sandstone. Overlain by Stairway Sandstone.|Very soft red to pink, finely laminated siltstone with interbedded medium- to coarse-grained, cross-bedded and well-sorted sandstone. Strongly weathered with common Fe-oxide mineral induration.|
8493|Horn Valley Siltstone|73346|6|Mentioned|p18|Middle Ordovician|Early Ordovician|Amadeus Basin. Includes the arandaspid Porophoraspis sp.||||||
8493|Horn Valley Siltstone|73567|6|Mentioned|p68|Ordovician|Ordovician|Amadeus Basin.||||||
8535|Howes Hill Lamproite|41158|6|Mentioned|Table 48|||||||||
8604|Hussar Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
8604|Hussar Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin||||||
8604|Hussar Formation|22907|6|Mentioned|41|||||||||
8604|Hussar Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
8604|Hussar Formation|23571|3|Fully described|p1, 8|Neoproterozoic|Neoproterozoic|Formerly known as the "Hussar beds". Geological Province: Officer Basin. Underlying Unit: Browne Formation (conformable). Overlying Unit: Kanpa Formation (conformable). Max. thickness: 897m. Contains stromatolites.||||||04-MAY-05
8604|Hussar Formation|24161|4|Described|p9 Fig.6, p11|Neoproterozoic|Neoproterozoic|Conformably overlies the Browne Formation. Conformably overlain by the Kanpa Formation. Geological Province: Officer Basin.||||||
8604|Hussar Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
8604|Hussar Formation|41751|6|Mentioned|p8|||||||||
8604|Hussar Formation|43756|6|Mentioned|p541|||||||||
8604|Hussar Formation|44111|6|Mentioned|p.59|||in Officer Basin. Includes Supersequence 1 palynological taxa.||||||
8604|Hussar Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
8604|Hussar Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: ~750Ma.  Geological Province: Officer Basin.||||||
8604|Hussar Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin. ||Unit in Buldya Group.|||Sandstone.|
8604|Hussar Formation|60118|6|Mentioned|p30|Neoproterozoic|Neoproterozoic|Contains halite beds <10m thick. Geological Province: Officer Basin.||||||
8604|Hussar Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. See also p16 Tb. 3.||||||11-APR-08
8604|Hussar Formation|61272|5|Briefly described|p120 Fig.1|||Overlies the Browne Formation. Overlain by Kanpa Formation.||||||
8604|Hussar Formation|61732|5|Briefly described|p4 Fig. 3, p58 Fig. 22|Torrensian|Willouran|Of the Buldya Group. Geological Province: Officer Basin. See also p131.||||||07-FEB-11
8604|Hussar Formation|62453|3|Fully described|p5 Fig. 3, 22, 27|Cryogenian|Cryogenian|Of Buldya Group. Geol. Prov: Officer Basin. Overlies: Browne Fm, Lancer Mbr. Correlated with Browne Fm. Underlies conformably: Kanpa Fm. Part of 'Woolnough Fm' now Hussar Fm. Sandstone, dolomite, limestone, siltstone, shale.||||||
8604|Hussar Formation|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
8604|Hussar Formation|63022|5|Briefly described|p1015, p1016 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Buldya Group. Overlain by Kanpa Formation; underlain by Browne Formation. Geological Province: Officer Basin. Brown sandstone, mudstone, and stromatolitic dolostone.||||||10-AUG-07
8604|Hussar Formation|64103|5|Briefly described|p400 Fig. 3, p404|Cryogenian|Cryogenian|Of Buldya Group. Geological Province: Officer Basin.||||||07-FEB-11
8604|Hussar Formation|64325|5|Briefly described|p80, p82 Fig. 2|Neoproterozoic|Neoproterozoic|A unit of Supersequence 1. Geological Province: western Officer Basin. Sandstone, dolomite, shale and minor evaporite deposits.||||||09-MAY-11
8604|Hussar Formation|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.||||||09-DEC-08
8604|Hussar Formation|64793|5|Briefly described|p283-293|Cryogenian|Cryogenian|Of central Officer Basin. Age inferred from Fig.3.|c.818 - c.770 Ma.|||Overlies Browne Formation. Is overlain by Kanpa Formation.|Sandstone, dolomite, mudstone; local conglomerate.|
8604|Hussar Formation|64796|5|Briefly described|p183 fig 2, p185, p200-201, p203|Neoproterozoic|Neoproterozoic|Of Officer Basin|||||Interbedded dolomite, mudstone, sandstone.|
8604|Hussar Formation|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
8604|Hussar Formation|64970|5|Briefly described|p717, p719 Fig. 2, p 721 Fig. 5, 6, 7.|Riphean|Riphean|Overlie Townsend Quartzite. Geological Province: Officer Basin.||||||27-MAY-09
8604|Hussar Formation|65102|4|Described|p365,366,367,371 Figs. 4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. 500-1000m; shale, dolomite, sandstone & siltstone. Eolian, arid inland drainage system; conformably overlies Browne Formation, conformably overlain by Kanpa Fm; type section in Yowalga 3, 991-1888m; contains palynomorphs indicating Riphean-Vendian age.||||||
8604|Hussar Formation|65363|3|Fully described|pp1-2, p6 Fig.5, pp9-10, pp18-19.|Neoproterozoic|Neoproterozoic|Officer Basin. Widespread unit, but shows little variation in facies. Type section is in drillhole Yowalga 3. Parts may correlate with upper Mundadjini Formation. The lithologies are described in detail. Excellent reservoir quality in the upper part, and the base of this Formation has a potential regional reservoir seal. Hydrocarbon traces were found to be almost entirely due to carbonate cements.|c.820 - 780 ma.|Unit in Buldya Group.||Overlies Browne Formation. Is overlain by Kanpa Formation.|Upper sandstone-dominated unit; an upper middle evaporitic mudstone and dolostone unit; a lower middle sandstone and dolostone unit; a lower evaporitic mudstone-dominated unit.|
8604|Hussar Formation|65364|5|Briefly described|p81|||Officer Basin.||||Overlain by Keene Basalt, underlain by Browne Formation.|Brown sandstone, mudstone and stromatolitic dolostone.|16-MAR-12
8604|Hussar Formation|65365|5|Briefly described|p3-7, p6 Fig. 2, p8 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group, western and central Officer Basin.  Includes stromatolite assemblage.||||||
8604|Hussar Formation|65366|5|Briefly described|p19, 20, 21, 23 Fig. 3, p24|Cryogenian|Cryogenian|Of the Buldya Group, western Officer Basin. Includes the Baicalia burra Stromatolite Assemblage||||||
8604|Hussar Formation|65368|5|Briefly described|p13, p15 Fig. 1, p16 Fig. 2|Neoproterozoic|Neoproterozoic|Pink and red sandstones and mudstones.||||||19-MAR-12
8604|Hussar Formation|65370|5|Briefly described|p39 Tb. 1, p40, 41, 42, 45|||In Lancer 1: grey, medium to coarse grained sandstone. Some dolomite cement. Black opaque globules observed in Hussar samples identified as contaminants. No evidence for oil, past or present.||||||04-MAY-11
8604|Hussar Formation|65371|5|Briefly described|p53, 54 Fig. 1, p55-57, p58|||Of Buldya Group, Officer Basin. Conformable on Browne Formation. Conformably overlain by Kanpa Formation. Sandstone, mudstone, stromatolitic dolostone, evaporitic mudstones.  V. shallow and marginal marine. Mineralogy discussed.||||||
8604|Hussar Formation|65410|6|Mentioned|p72, p76, p78.|Neoproterozoic|Neoproterozoic|Western Officer Basin. Part of Supersequence 1. Contains a palynological assemblage of large acritarchs resembling Cerebrosphaera, coenobial aggregates and leiospheres.||||||
8604|Hussar Formation|65416|5|Briefly described|p137, p138 Fig.3, p141.|Late Proterozoic|Late Proterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Shallow-marine or sabkha, and beach to eolian environments. Eolian-dune sandstones have 12-21% porosities: the primary petroleum reservoir targets in the Basin; sealed by Kanpa Formation shales.||||Overlies Browne Formation conformably. Is overlain conformably by Kanpa Formation.|Interbedded siltstone, shale and sandstone with thin beds of dolomite and limestone.|
8604|Hussar Formation|67195|4|Described|p9 fig 5, p10, p19 tbl 1, p44, 45, 47|Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.99 W/mK. Basal unit of one well in this study. See also App 1.||||Overlies Browne Formation, overlain by Kanpa Formation|fine to coarse grained, sometimes cross-bedded sandstones, interbedded with laminated siltstone, dolomite (with soft sediment deformation), shale and mudstone.|04-JAN-23
8604|Hussar Formation|67200|5|Briefly described|app 2 p9||||||||Dolomite and interbedded mudstone, siltstone and sandstone.|
8604|Hussar Formation|67454|4|Described|p563, pp564-567, p569, p571.|Neoproterozoic|Neoproterozoic|Officer Basin. Correlated with Burra Group (South Australia). Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed.|c.800 - 760 Ma.|Unit in Buldya Group.||Overlies Browne Formation. Is overlain conformably by Kanpa Formation.|Lower half predominantly mudstone; minor interbedded sandstone, dolostone and evaporite. Upper half mainly sandstone; minor interbedded mudstone and dolostone.|
8604|Hussar Formation|68275|6|Mentioned|p57|||||||||
8604|Hussar Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
8604|Hussar Formation|69029|6|Mentioned|p328-330|Neoproterozoic|Neoproterozoic|Of Officer Basin. Contains thin organic-rich source rock shales ranging from fair to good oil potental.||||Overlain by Kanpa Formation. Underlain by Browne Formation.||
8604|Hussar Formation|69091|5|Briefly described|p30 Fig.3.5, p38 Fig.3.7, see comments|Neoproterozoic|Neoproterozoic|Officer Basin. See also p41 Fig.3.8, p44, p81 Fig.4.17, p108 Fig.5.9, p115 Fig.5.14, p174 Fig.9.5, p177 Fig.9.6, p182, p200 Fig.10.2.||Buldya Group||Is unconformably overlain by Table Hill Volcanics.|Sedimentary.|26-SEP-14
8604|Hussar Formation|69152|4|Described|500k_geologyp08_lut||Neoproterozoic|||Buldya Group|||Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.|06-AUG-15
8604|Hussar Formation|70153|6|Mentioned|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian|||Buldya Group||||
8604|Hussar Formation|70793|5|Briefly described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.||Unit of Buldya Group.||||
8604|Hussar Formation|71001|6|Mentioned|p22|||Officer Basin.||||Overlies Browne Formation.|Transgressive sequence of shallow-marine, evaporitic dolostone and mudstone.|
8604|Hussar Formation|71268|5|Briefly described|100k_interpgeop_lut.csv|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.||Unit of Buldya Group.||||
8604|Hussar Formation|71270|5|Briefly described|500k_interpgeop16_lut.csv|Tonian|Tonian|Of Officer Basin, Centralian Superbasin.||Unit of Buldya Group.||||
8604|Hussar Formation|71288|6|Mentioned|p136-137|Neoproterozoic|Neoproterozoic|An 800-730 Ma paleopole position from this unit locates Australia in low latitudes.|800-730 Ma.|||||
8604|Hussar Formation|71800|5|Briefly described|p26-p27|Ediacaran|Ediacaran|Officer Basin.||||Overlies the Wahlgu Formation. Overlain by the Lupton Formation.|Sandstone.|
8604|Hussar Formation|73086|6|Mentioned|p57|||Officer Basin.||||May be partly correlative to Wallara Formation.||
8652|Illagie Iron-Formation Member|38978|6|Mentioned|p155|||||||||
8652|Illagie Iron-Formation Member|40938|4|Described|p29|||||||||
8665|Illimbirrie Formation|29690|3|Fully described|p8|||||||||
8665|Illimbirrie Formation|30949|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
8669|Ilma Formation|41751|6|Mentioned|p8|||||||||
8669|Ilma Formation|43442|6|Mentioned|p20||Proterozoic|||||||
8669|Ilma Formation|62453|3|Fully described|p5 Fig. 3, 10, 39, 41|Cryogenian|Cryogenian|Of the Buldya Group. Geological Province: Officer Basin. Dolomite with minor limestone, chert and sandstone. Overlain by Mason Conglomerate. Correlated with Neale Formation. Overlian by Colville Formation.||||||
8669|Ilma Formation|62987|5|Briefly described|p30|||Probably of the Buldya Group? Geological Province: Officer Basin.||||||25-JAN-07
8669|Ilma Formation|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Formation is Fm in text. Geological Province: Officer Basin.||||||07-FEB-11
8669|Ilma Formation|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Of Buldya Group. Oolitic dolomite, stromatolitic and sandy; minor limestone, chert, and sandstone, shaly with evaporite pseudomorphs in subsurface.||||||09-DEC-08
8669|Ilma Formation|65102|4|Described|p365,366,367,372, Figs.4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. 10-500?m; Ilma & Neale Fms may correlate with Lefroy Fm or overlie it. Stromatolitic and oolitic dolomite, limestone, chert and sandstone; shallow marine, part intertidal; base of unit not seen; type section at 29deg 49min 05sec S, 126deg 12min 33sec E; contains baicalia cf. burra.||||||
8669|Ilma Formation|65366|6|Mentioned|p22 Fig.2|||? Officer Basin||||||19-MAR-12
8669|Ilma Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Western Officer Basin. Part of Supersequence 1.||||||
8669|Ilma Formation|65416|6|Mentioned|p140.|||||||||
8669|Ilma Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
8669|Ilma Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||limestone, crystalline dolostone/dolomite, chert, sandstone|
8669|Ilma Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Officer Basin (Phase 1).||Buldya Group|||Oolitic dolomite, stromatolitic and sandy; minor limestone, chert, and sandstone, shaly with evaporite pseudomorphs in subsurface.|
8684|Indulkana Shale|22746|5|Briefly described|Fig.3 p515|Ordovician|Ordovician|||||||
8684|Indulkana Shale|22922|6|Mentioned|34|||||||||
8684|Indulkana Shale|23282|2|Defined|p82||Late Ordovician|Informally introduced by Packham and Webby (1969) and use by Krieg (1973). Probably equiv. to Horn Valley Siltstone of Amadeus Basin. Age: Late Ordovician 450 - 455 Ma. of Munda Group, Officer Basin.||||||
8684|Indulkana Shale|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
8684|Indulkana Shale|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|||||||
8684|Indulkana Shale|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
8684|Indulkana Shale|24067|5|Briefly described|p249 Fig.2|Ordovician|Ordovician|Geological Province: Officer Basin.||||||
8684|Indulkana Shale|24112|5|Briefly described|p254 Fig.2|Late Ordovician|Late Ordovician|Of the Munda Group. Geological Province: Officer Basin||||||
8684|Indulkana Shale|30540|6|Mentioned|p68|||Possible source rock||||||
8684|Indulkana Shale|30544|6|Mentioned|p49|||||||||
8684|Indulkana Shale|30807|6|Mentioned|p102|||Suggested map symbol.||||||
8684|Indulkana Shale|31457|6|Mentioned|p13|||||||||
8684|Indulkana Shale|31698|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|?Lower to ?Middle Ordovician||||||
8684|Indulkana Shale|33738|6|Mentioned|p48|||||||||
8684|Indulkana Shale|35628|4|Described|Table 3|||||||||
8684|Indulkana Shale|36096|6|Mentioned|Fig.3|||||||||
8684|Indulkana Shale|36128|6|Mentioned|p13|||||||||
8684|Indulkana Shale|36491|6|Mentioned|Fig.2|||||||||
8684|Indulkana Shale|36920|6|Mentioned|Table 1|||||||||
8684|Indulkana Shale|38022|6|Mentioned|Fig.4|||||||||
8684|Indulkana Shale|38329|6|Mentioned|p194|||||||||
8684|Indulkana Shale|40136|5|Briefly described|p28|||||||||
8684|Indulkana Shale|43052|5|Briefly described|Fig. 2.10|||||||||
8684|Indulkana Shale|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
8684|Indulkana Shale|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
8684|Indulkana Shale|43732|6|Mentioned|Fig.4,p5||Early Ordovician|||||||
8684|Indulkana Shale|43743|6|Mentioned|Fig.2,p33||Late Ordovician|||||||
8684|Indulkana Shale|44109|5|Briefly described|p22 Fig. 23|Ordovician|Ordovician|Geological Province: central Officer Basin.||||||
8684|Indulkana Shale|44133|4|Described|p40-41, 4 Fig. 7.2|Ordovician|Ordovician|Geological Province: Eastern Officer Basin. Of the 'Munda Sequence'. Overlies Mount Chandler Sandstone. Maximum Thickness: 60m. Age: 460 +/- 15-438 +/- 10 Ma (Webb, 1978, Womer et al , 1987). Underlies: Blue Hills Sandstone.||||||02-MAY-13
8684|Indulkana Shale|45149|6|Mentioned|p43|||See also Table 1 and P15.||||||
8684|Indulkana Shale|49792|5|Briefly described|Fig.5|||||||||
8684|Indulkana Shale|65313|5|Briefly described|p578, p579, p580 Fig. 6|Ordovician|Ordovician|Officer Basin. Ungoolya 1 well. ca 468 Ma from Horn Valley Sandstone correlation 460 +/- 15 Ma Rb-Sr isochron date.||Of Munda Group.||Overlies Mount Chandler Sandstone, underlies Blue Hills Sandstone.||26-MAR-12
8684|Indulkana Shale|71146|5|Briefly described|p6|Late Ordovician|Middle Ordovician|Officer Basin.||Munda Group||Overlies the Mount Chandler Sandstone. Overlain by the Blue Hills Sandstone.|Shale.|
8684|Indulkana Shale|72478|6|Mentioned|p8|Late Ordovician|Late Ordovician|Officer Basin.|c.450 Ma-445 Ma|Munda Group||Overlies the Mt Chandler Sandstone. Underlies the Blue Hills Sandstone.||25-MAR-21
8684|Indulkana Shale|73090|5|Briefly described|p12 Fig.7, Appendix|Silurian|Ordovician|||Munda Group.|||Shale, maroon, minor green, calcareous; thin white flaggy siliceous sandstone interbeds; rare limestone lenses. Rippled, dessicated, bioturbated.|
8774|Iron King Member|24165|5|Briefly described|p76|Archean|Archean|Iron King Mine, 5km SSE of Norseman. Mined for pyrite as a source of sulfur.||Noganyer Formation.||||
8774|Iron King Member|30562|4|Described|p38|||Of Noganyer Formation.||||||27-NOV-09
8774|Iron King Member|43162|6|Mentioned|6|||||||||
8786|Irregully Formation|22694|5|Briefly described|p8|||||||||
8786|Irregully Formation|22897|6|Mentioned|103|||Geol province Bangemall Basin||||||
8786|Irregully Formation|22905|5|Briefly described|p52 Fig. 2, p53|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Overlying unit: Gooragoora Formation; underlying unit: Ashburton Formation and Capricorn Formation.  Max. thickness: 1200m.||||||24-JAN-06
8786|Irregully Formation|22940|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of the Bangemall Group. Overlain by Jillawarra Formation.||||||12-SEP-07
8786|Irregully Formation|23280|6|Mentioned|Table1p1085|||||||||
8786|Irregully Formation|23310|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group.||||||
8786|Irregully Formation|23311|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Bangemall Group.||||||
8786|Irregully Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Bangemall Group.||||||
8786|Irregully Formation|23403|4|Described|p7|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Consists of dolomite with thin interbeds of quartz arenite, pebble conglomerate and shale.||||||24-NOV-09
8786|Irregully Formation|23485|4|Described|p30|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.||||||07-NOV-08
8786|Irregully Formation|23487|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Geological Province: Edmund Basin.||||||07-NOV-08
8786|Irregully Formation|23525|4|Described|p29|Paleoproterozoic|Paleoproterozoic|Of the Edmund Group.||||||07-NOV-08
8786|Irregully Formation|23527|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group, Edmund Basin||||||
8786|Irregully Formation|23723|4|Described|p9 Table 1|Mesoproterozoic|Mesoproterozoic|Of Bangemall Group. O'lying unit Glen Ross Shale Member. U'lying unit Tringadee Formation. Geol. Province: Bangemall Basin. Max. thickness: 2000 m.||||||22-MAY-08
8786|Irregully Formation|24115|4|Described|p4 Fig.2|Mesoproterozoic|Mesoproterozoic|Of the Edmund Group. Maximum Thickness: 1200m. Overlies the Yilgatherra Formation. Overlain by the Gooragoora Formation. Geological Province: Edmund Basin.||||||
8786|Irregully Formation|24183|2|Defined|p4 Fig.3, p7, p8|Calymmian|Statherian|Conformably overlies the Yilgatherra Formation. Max. Thickness: >2000m. Contains stromatolites. Overlain by the Gooragoora, Blue Billy & Kiangi Creek Formations. Age: 1620-1462 Ma. Youngest detrital zircon population: 1805 Ma.||||||21-MAR-11
8786|Irregully Formation|24544|4|Described|p44 Fig.32|Mesoproterozoic|Mesoproterozoic|Base of Bangemall Supergroup. Of Edmund Group. Conformably overlies Coobarra Formation. Overlain by Gooragoora Formation. Max. thickness: 500 m. Dolarenite and dololutite. Contains stromatolites. Coastal lagoon depositional enironment.||||||
8786|Irregully Formation|29845|6|Mentioned|p183|||||||||
8786|Irregully Formation|29916|4|Described|p115|||||||||
8786|Irregully Formation|30880|6|Mentioned|p529|||||||||
8786|Irregully Formation|30881|4|Described|p525|||||||||
8786|Irregully Formation|31022|6|Mentioned|Fig. 1|||Stromatolites||||||
8786|Irregully Formation|31154|6|Mentioned|p70|||||||||
8786|Irregully Formation|32720|6|Mentioned|Table 1|||||||||
8786|Irregully Formation|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
8786|Irregully Formation|32727|6|Mentioned|p10|||Dates||||||
8786|Irregully Formation|34066|6|Mentioned|p10|||M.Prot.||||||
8786|Irregully Formation|34124|5|Briefly described|Table 1|||Upper Proterozoic. See also PP7,8,14||||||
8786|Irregully Formation|34202|6|Mentioned|p1056|||||||||
8786|Irregully Formation|34999|6|Mentioned|Table 17|||||||||
8786|Irregully Formation|35052|6|Mentioned|p18|||||||||
8786|Irregully Formation|35639|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8786|Irregully Formation|35982|6|Mentioned|Table 22|||||||||
8786|Irregully Formation|36551|6|Mentioned|p101|||||||||
8786|Irregully Formation|36884|3|Fully described|p148|||||||||
8786|Irregully Formation|36902|6|Mentioned|p16|||||||||
8786|Irregully Formation|37024|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8786|Irregully Formation|37213|5|Briefly described|p22|||||||||
8786|Irregully Formation|37460|4|Described|p160|||||||||
8786|Irregully Formation|38298|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
8786|Irregully Formation|38299|5|Briefly described|p9|||||||||
8786|Irregully Formation|38482|6|Mentioned|p16|||See also Table 5.||||||
8786|Irregully Formation|38493|6|Mentioned|p31|||||||||
8786|Irregully Formation|38988|6|Mentioned|p12|||||||||
8786|Irregully Formation|39210|5|Briefly described|Table 2|||||||||
8786|Irregully Formation|39370|4|Described|p31|||||||||
8786|Irregully Formation|40088|4|Described|p224|||||||||
8786|Irregully Formation|40089|2|Defined|p21|Mesoproterozoic|Mesoproterozoic|See also p13.||||||12-SEP-07
8786|Irregully Formation|40899|6|Mentioned|Fig.1|||||||||
8786|Irregully Formation|41144|6|Mentioned|Table 1|||||||||
8786|Irregully Formation|41360|6|Mentioned|p191|||||||||
8786|Irregully Formation|42013|5|Briefly described|Map Legend|Proterozoic||||||||
8786|Irregully Formation|42471|4|Described|p19|||||||||
8786|Irregully Formation|42472|5|Briefly described|Map legend|||||||||
8786|Irregully Formation|43256|6|Mentioned|16||Proterozoic|||||||
8786|Irregully Formation|43830|5|Briefly described|Map Legend||Mesoproterozoic|||||||
8786|Irregully Formation|44142|4|Described|p311, p313-314 Tb.4-4, p317|||See also p318-320, p326-327 Tb.4-5. Up to 1300m thick of deposits from fringing coastal lagoon system, tidal flats, shoals and washover fans. Contains stromatolites. In places overlies directly Ashburton Basin and Gascoyne Complex. On the WYLOO map was divided into 9 Members by Daniels (1970). Within Weegarinna Subgroup (of Chuck 1984). Stratigraphically equivalent rocks dated 1.5-1.6 Ga.||Basal Edmund Subgroup.||Overlies Tringadee Formation conformably and Ashburton Formation (angular-) unconformably. Overlain conformably by Gooragoora Sandstone and Kiangi Creek Formation.|Dolomite shale, siltstone; minor sandstone. Abundant stromatolitic beds in the carbonates are a feature of this unit.|13-MAR-18
8786|Irregully Formation|44319|14|Not recorded|map legend||Mesoproterozoic|Bangemall Group. M.Proterozoic.||||||
8786|Irregully Formation|50225|3|Fully described|p387 Fig. 2, p390|||Of the Edmund Group (Bangemall Supergroup). Conformably overlies Yilgatherra Formation. Stromatolitic and laminated dolostone. Max. thickness: >3km. Type section is in the Irregully Gorge.||||||07-FEB-11
8786|Irregully Formation|50226|5|Briefly described|p428, p429|||Of the Edmund Group.  Has mineralised horizons.||||||
8786|Irregully Formation|50292|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Edmund Basin.  Of the Edmund Group (Bangemall Supergroup). Overlies: Yilgatherra Formation.  Underlies: Gooragoora Formation.||||||07-NOV-08
8786|Irregully Formation|50312|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Overlies Yilgatherra Formation. Overlain by Gooragoora Formation. Geological Province: Edmund Basin. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.||||||31-MAY-04
8786|Irregully Formation|50313|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup).  Geological Province: Edmund Basin. Underlies: Gooragoora Formation.||||||07-NOV-08
8786|Irregully Formation|50380|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin.||||||07-NOV-08
8786|Irregully Formation|60301|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. dolostone, dolomitic siltstone, quartz sandstone and conglomerate.||||||07-NOV-08
8786|Irregully Formation|61270|5|Briefly described|p91, p93, p94 Tb.1|Mesoproterozoic|Mesoproterozoic|Of Edmund Subgroup. Redefined to include only the basal sequence, the overlying sequence being excluded. Overlies Capricorn Fm. Thickness at type section: 345m. Dolomite with minor silicalstic rock; stromatolites abundant. Geol. Prov: Bangemall Basin.||||||
8786|Irregully Formation|61273|5|Briefly described|p85|Mesoproterozoic|Mesoproterozoic|Contains high-grade dolomitic marble which is quarried for dimension stone.||||||
8786|Irregully Formation|62428|5|Briefly described|p336|||Of the lower Bangemall Group. Intruded by an olivine gabbro dyke of the Mundine Well dyke swarm.||||||10-FEB-09
8786|Irregully Formation|63469|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of Edmund Group. Includes stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone and conglomerate.||||||24-SEP-07
8786|Irregully Formation|63470|5|Briefly described|Map legend||Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Geological Province: Edmund Basin. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.||||||07-NOV-08
8786|Irregully Formation|63471|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Edmund Group (Bangemall Supergroup). Overlies Mount Augustus Formation; underlies Devil Creek Formation. Geological Province: Edmund Basin. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone and conglomerate.||||||07-NOV-08
8786|Irregully Formation|63866|5|Briefly described|p162|||||Edmund Group||||
8786|Irregully Formation|63869|4|Described|p28-31, p37, p42, p44, p45, p51, p53|Calymmian|Statherian|See also p59-60, Plate 1. Of Daniels (1966), a revision of Top Camp Dolomite. Originally included all units below Kiangi Creek Formation. Revised by Chuck (1984) and Copp (1998); now includes only the lower dolostone interval (Wongida Dolomite Member) of original Irregully Formation. 350-2000 m thick. Inferred age from regional stratigraphic relationships. Hosts local Cu, Pb and Zn mineralisation. Quarried for green dolomitic marble dimension stone.|c.1620-1465 Ma.|Unit in Edmund Group.||Conformably overlies Yilgatherra Formation. Unconformably overlies Wyloo Group and Gascoyne Complex. Is overlain disconformably by Kiangi Creek Formation.|Laminated and stromatolitic dolostone and dolorudite; minor sandstone and dolomitic sandstone; rare conglomerate and laminated siltstone.|
8786|Irregully Formation|64287|4|Described|p31, p32, p34 Fig. 2|||Basal unit Edmund Gp - redef.to incl.only lowermost major carbonate unit, Wongida Dolomite Member (Daniels 1970) and hisYilgatherra Mbr now elevated to formation status. Unconformably overlies basement where Yilgatherra Fm.absent. Detailed lith.included||||||07-FEB-11
8786|Irregully Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone, and conglomerate.||||||09-DEC-08
8786|Irregully Formation|64728|5|Briefly described|pp95-97, pp101-102, p107.|Mesoproterozoic|Mesoproterozoic|Fluvial to shallow marine siliciclastic and carbonate facies. Sediments eroded from Ashburton Formation and coeval Moorarie Supersuite, or younger derivatives of these; and from Durlacher Supersuite.|Maximum depositional age c.1767-1785 +/- 7 Ma.|Unit in Edmund Group.||Overlies Yilgatherra Formation. Is overlain by Gooragoora Formation.|Dolomitic sandstone.|
8786|Irregully Formation|65453|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Over Yilgatherra Formation; under Kiangi Creek Formation. Stromatolitic and non-stromatolitic dolostone, dolomictic siltstone, quartz sandstone and conglomerate. Geol. Prov: Edmund Basin.||||||
8786|Irregully Formation|65545|5|Briefly described|Map Legend|Mesoprotoerozoic|Paleoproterozoic|Of Edmund Group, Edmund Basin. Age: c. 1460 - <1620 Ma. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.||||||
8786|Irregully Formation|65549|5|Briefly described|Map Legend|Calymmian|Statherian|Of Edmund Group, Bangemall Supergroup, Edmund Basin. Underlies Kiangi Creek Formation; overlies Yilgatherra Formation. Stromatolitic and non-stromatolitic dolostone, dolomitic sandstone, quartz sandstone, and conglomerate.||||||06-SEP-10
8786|Irregully Formation|65830|4|Described|p4, p5, p9, p13-14, p21-23, Plate 1,2|Calymmian|Statherian|~350 m-2000 m thick. Intertidal to shelf and slope carbonate rocks and interbedded fluvial to shallow-marine siliciclastic rocks. Unconformably underlain by the Ashburton Formation.||Of the Edmund Group||Conformably overlies Yilgatherra Formation. Disconformably overlain by the Gooragoora Formation, Blue Billy Formation. Disconformably overlain by the Kiangi Creek Formation.|Consists of laminated and stromatolitic dolostone and dolorudite, minor sandstone, and dolomitic sandstone with rare conglomerate.|
8786|Irregully Formation|65896|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in lower Edmund Group, Bangemall Supergroup. Stromatolitic and non-stromatolitic dolostone; grey, fine-planar, parallel-laminated dolomitic siltstone, siltstone, and silty sandstone.||||||
8786|Irregully Formation|66104|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in lower Edmund Group. Stromatolitic and non-stromatolitic dolostone; dolomitic siltstone, quartz sandstone and conglomerate.||||||
8786|Irregully Formation|66105|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of Edmund Group. Overlies Yilgatherra Formation and underlies Kiangi Creek Formation. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone and conglomerate. Includes two unnamed units of sandstone, siltstone and dolostone.||||||
8786|Irregully Formation|66110|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate. Includes an unnamed unit of sandstone, conglomerate, siltstone and dolostone.||||||
8786|Irregully Formation|66112|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Unit in Edmund Group. Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.||||||
8786|Irregully Formation|66241|4|Described|pp1-5, pp10-12. |||Correlates with the Gap Well Formation. Thickness increases north-to-south from 350 m to over 3000 m. Hosts the Abra polymetallic deposit.||Unit in Edmund Group.||Conformably overlies Yilgatherra Formation. Is overlain by Gooragoora Formation.|Mainly laminated and stromatolitic dolostone and dolorudite, and dolomitic sandstone; sandstone and siltstone are interbedded with the dolostone in the southern Edmund Basin.|
8786|Irregully Formation|66299|5|Briefly described|p69, p127.|Mesoproterozoic|Paleoproterozoic|||Unit in Edmund Group.||Unconformably overlies Leake Spring Metamorphics.|Dolostone.|
8786|Irregully Formation|66579|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin||Unit in Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|67136|5|Briefly described|Map legend.|||Edmund Basin. Includes two un-named but separately mapped units.||Unit in Edmund Group.||In cross-section, overlies Bresnahan Group, and is overlain by Blue Billy Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, conglomerate.|14-NOV-11
8786|Irregully Formation|67245|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin. Includes three other separately-mapped but un-named sub-units.||Unit in Edmund Group.|Includes Woodlands Member.|Overlies Yilgatherra Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|67246|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes four un-named sub-units which are mapped separately.||Unit in Edmund Group.||Overlies Yilgatherra Formation. Is intruded by Narimbunna Dolerite. Is overlain by Kiangi Creek Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|19-NOV-13
8786|Irregully Formation|67247|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Shown as part of 'Depositional package 1' in the interpreted bedrock geology map legend.||Unit in Edmund Group.||||20-NOV-13
8786|Irregully Formation|67371|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Edmund Basin.||Unit in Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone and conglomerate; minor unit of sandstone, conglomerate, siltstone and dolostone.|
8786|Irregully Formation|67374|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin.||Unit in Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|68285|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Base of unit shown as <1620 Ma. Presumably because not affected by Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES) ||Of the Edmund Group.|Informally subdivided in part into three unnamed units.|Unconformably underlain by the Bresnahan Group or Ashburton Formation, Wyloo Group. Overlain by Blue Billy Formation or Kiangi Creek Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate; siltstone and  sandstone; minor dolostone; sandstone, conglomerate, siltstone, and dolostone; thick-bedded quartz sandstone; minor siltstone.|
8786|Irregully Formation|68286|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Base of unit shown as <1620 Ma. Presumably because not affected by Mangaroon Orogeny (1677-1619 Ma, Sheppard, 2005 AJES) ||Of the Edmund Group|Informally subdivided in part into two unnamed units.|Unconformably underlain by the Ashburton Formation. Overlain by the Blue Billy Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|68521|5|Briefly described|Map Legend|Statherian|Statherian||c.1620 Ma|Of the Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|68522|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin.|<1620 - c.1465 Ma|Of the Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|69003|5|Briefly described|p34, p42|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen. Hosts the giant Abra polymetallic deposit (described).||Edmund Group.||Overlies Yilgatherra Formation. Is overlain by Gooragoora Formation.||
8786|Irregully Formation|69024|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Of the Edmund Group.||Overlies Yilgatherra Formation. Is overlain by Gooragoora Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone and conglomerate.|05-MAY-14
8786|Irregully Formation|69027|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin. Includes an unnamed subunit comprising sandstone, conglomerate, siltstone, and dolostone.||Of the Edmund Group.||Underlain by the Yilgatherra Formation. Overlain by the Gooragoora Formation.|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|05-MAY-14
8786|Irregully Formation|69028|5|Briefly described|Map Legend|Calymmian|Statherian|Edmund Basin. Mapped with Yilgatherra Formation as one unit.||Of the Edmund Group.|||Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, sandstone, siltstone and conglomerate.|06-MAY-14
8786|Irregully Formation|69166|4|Described|geologyp_lut.csv|Mesoproterozoic|Paleoproterozoic|Age derived from dolomitic quartz sandstone sample (148969.1.pdf)|1772 Ma +/- 10 Ma (SHRIMP)|Edmund Group|Includes Woodlands Member, Yilgatherra Member|Conformably overlies Yilgatherra Formation, Conformably overlain by Gooragoora Formation, unconformably overlain by Blue Billy Formation, Kinagi Creek Formation|Stromatolitic and non-stromatolitic dolostone, dolomitic siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|||Part of Edmund Group, Depositiional package 1.||Unit of Edmund Group.||||
8786|Irregully Formation|69583|5|Briefly described|Plate 3|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||||
8786|Irregully Formation|69596|6|Mentioned|p12 Fig.7|||Edmund Basin.||Edmund Group.||||
8786|Irregully Formation|70019|4|Described|p92-96,108|Mesoproterozoic|Mesoproterozoic|Geological province: Gascoyne Province, Capricorn Orogen. Intruded by mafic sills of Waldburg Dolerite, thereby providing minimum age of deposition of this untit. Base of Irregully Formation in the Abra region is not exposed, thickness and relationship to underlying units are not known. Hosts main mineralisation of the Abra polymetallic (Fe, Pb, Zn, Ba, Cu, Au, Ag, Bi, and W) deposit. Main 207Pb/206Pb age population with a weighted mean age of 1594+\-10 Ma of xenotime from the Black Zone in the Irregully Formation. Hydrothermal events at c. 1375 and 1220 Ma recorded by hydrothermal xenotine grains in the Balck Zone of irregullly Formation, and by a Re-Os model age at 1284+\-47 Ma from pyrite in the Red Zone. ||Unit of Edmund Group.||Overlain by Gooragoora Formation. Underlain by Yilgatherra Formation.|Laminated and stromatolitic dolostone and dolorudite, and dolomitic sandstone, locally with siltstone and fine-grained sandstone.|
8786|Irregully Formation|70127|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.||Edmund Group.|||Stromatolitic and non-stromatolitic dolostone; minor siltstone and sandstone.|
8786|Irregully Formation|70132|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Edmund Basin.|<1679 Ma.|Edmund Group.||Is overlain by Kiangi Creek Formation.|Stromatolitic and non-stromatolitic dolostone, siltstone, quartz sandstone and conglomerate (section only).|
8786|Irregully Formation|70138|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.||Overlies Yilgatherra Formation. Is overlain by Gooragoora Formation.|Stromatolitic and non-stromatolitic dolostone; minor siltstone and sandstone.|
8786|Irregully Formation|70767|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin. Section only: no outcrop in map area.|<1679 Ma.|Edmund Group.||Unconformably overlies Bresnahan Group. Is overlain by Blue Billy or Kiangi Creek Formations.|Stromatolitic and non-stromatolitic dolostone, siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|70768|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Edmund Basin. Section only: no outcrop in map area.|<1679 Ma.|Edmund Group.||Unconformably overlies Bresnahan Group. Is overlain by Blue Billy or Kiangi Creek Formations.|Stromatolitic and non-stromatolitic dolostone, siltstone, quartz sandstone, and conglomerate.|
8786|Irregully Formation|70795|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|Also 100k_geologyl_lut.csv, 100k_interpgeop_lut.csv, 148969.1.pdf, 149028.1.pdf, West Australian Craton, Edmund Basin|1679-1610 Ma|Edmund Group|Includes Woodlands Member, Yilgatherra Member|Includes Woodlands Member, Yilgatherra Member, intruded by Waldburg Dolerite|Siltstone and thin- thick bedded sandstone, dolomitic quartz sandstone, stromatolitic and non stromatolitic dolostone, metasandstone, minor dolomitic siltstone.|
8786|Irregully Formation|70814|4|Described|p3, p5, p7-p9, p20|Statherian|Statherian|Edmund Basin. Together with the Yilgatherra Formation forms Depositional Package 1 of the Edmund Group. Along with the Gooragoora Formation hosts the Abra polymetalic deposit. On the Pingandy Shelf this unit is generally 300-400m thick however south of the Talga Fault it reaches a maximum thickness of 3600m. Age is derived from the maximum age of the underlying Mount Augustus Sandstone. Unconformably overlies the Wyloo, Capricorn and Bresnahan Groups. Disconformably overlain by the Blue Billy Formation. Conformably overlain by the Gooragoora Formation. Intruded by the Waldburg Dolerite. See also  p22, p24-p25, p31, p41, p47, p49, p53.|1679-1610 Ma|Edmund Group||Conformably overlies the Yilgatherra Formation. Disconformably overlies the Moorarie Supersuite. Unconformably overlain by the Kiangi Creek Formation.|Carbonates and stromatolitic shelf dolomites, interbedded with minor siliciclastic sedimentary rocks.|04-MAY-23
8786|Irregully Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dololutite, siltstone, sandstone, crystalline dolostone/dolomite|
8786|Irregully Formation|71273|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Edmund Basin.||Edmund Group.|||Sandstone with subordinate conglomerate, siltstone and dolostone; stromatolitic and non-stromatolitic dolostone with minor siltstone and sandstone.|
8786|Irregully Formation|72705|5|Briefly described|p3-6, 10-12|Mesoproterozoic|Mesoproterozoic|Capricorn Orogen.||Edmund Group.||Conformably overlies Yilgatherra Formation. Is overlain conformably by Gooragoora Formation.|Detrital and carbonate sedimentary rocks.|
8786|Irregully Formation|72758|5|Briefly described|p50-53, p8-9 Tb.1.|||Formation c. 2800m thick.||Bangemall Group|Yilgatherra Member, Wongida Dolomite Member, Gooragoora Sandstone, Wannery, Chubilyer Members, Weewoddie Dolomite Member, Yeelingee Member, Warrada Dolomite Member, Revels Corner Sandstone Member.|Unconformably overlies Morrissey Metamorphic Suite, Mount Minnie Group and conformably underlies Kiangi Creek Formation.|Massive white weathering dolomite overlain by well bedded dolomite, chert and abundant silicified stromatolites. Mudstone (dominant in south of Parry Range) and thin sandstone. Thin bedded, cross stratified sandstone and iron oxide pseudomorphs.|
8799|Isdell Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Lamil Group, Yeneena Basin.||||||
8799|Isdell Formation|23746|5|Briefly described|p7|||Of Lamil Group.||||||
8799|Isdell Formation|23758|6|Mentioned|p5|||||||||
8799|Isdell Formation|23760|4|Described|p25|Proterozoic|Proterozoic|Of Lamil Group. Geological Province: Yeneena Basin.||||||
8799|Isdell Formation|23900|4|Described|p1537 Fig.2|Proterozoic|Proterozoic|Of the Lamil Group. Unconformably overlies the Broadhurst Formation. Overlain by the Malu Quartzite. Geological Province: Paterson orogen.||||||
8799|Isdell Formation|24194|5|Briefly described|p900 Fig.3|||Dolo-arenite and dolo-lutite with minor sandstone, shale and conglomerate. Parent: Lamil Group. Geological Province: Paterson Orogeny||||||
8799|Isdell Formation|24594|5|Briefly described|p601|Neoproterozoic|Mesoproterozoic|Of the Lamil Group.  Carbonate and pelitic rocks.  Geological Province: Yeneena Basin (Paterson Orogen).||||||
8799|Isdell Formation|33849|4|Described|p126|||||||||
8799|Isdell Formation|36551|6|Mentioned|Table 22|||||||||
8799|Isdell Formation|36632|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8799|Isdell Formation|37023|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8799|Isdell Formation|37212|3|Fully described|p13|||||||||
8799|Isdell Formation|37214|6|Mentioned|p6|||||||||
8799|Isdell Formation|37460|4|Described|Table3.VII|||||||||
8799|Isdell Formation|37707|6|Mentioned|Table I|||||||||
8799|Isdell Formation|41669|4|Described|p48|||||||||
8799|Isdell Formation|42278|6|Mentioned|p33|||||||||
8799|Isdell Formation|42352|6|Mentioned|p29|||Part of Yeneena Group||||||
8799|Isdell Formation|42702|5|Briefly described|map legend|Proterozoic||||||||
8799|Isdell Formation|43055|4|Described|p28, Table 4|||Of Yeneena Group.||||||09-DEC-08
8799|Isdell Formation|43056|5|Briefly described|Map Legend|||of Yeneena Group||||||
8799|Isdell Formation|43118|4|Described|p23|||Of Yeneena Group.||||||09-DEC-08
8799|Isdell Formation|43278|5|Briefly described|p644,Fig.2.|Neoproterozoic|Neoproterozoic|of Yeneena Group.||||||
8799|Isdell Formation|43348|4|Described|P10, p12|||||||||
8799|Isdell Formation|43862|5|Briefly described|Fig.2 p378|||||||||
8799|Isdell Formation|43867|5|Briefly described|p199,201|||||||||
8799|Isdell Formation|43868|5|Briefly described|Fig.3 p154|||||||||
8799|Isdell Formation|44139|5|Briefly described|p277-280, p282|Neoproterozoic|Neoproterozoic|Williams et al. (1976). Western, central and northeastern zones of Yeneena Basin. 2000 m. Dolomite, dolomitic shale; minor sandstone, shale, conglomerate. Contains stromatolites. Appears to disconformably overlie, and is faulted against, Choorun Formation; disconformably overlies Broadhurst Fms, conformably overlain by Malu Quartzite, and south of Telfer, by the Telfer Formation.| | ||||05-MAR-18
8799|Isdell Formation|44190|5|Briefly described|Map Legend||Proterozoic|||||||
8799|Isdell Formation|50436|5|Briefly described|p4.1|||Of the Yeneena Supergroup. Geological Province: Paterson Orogen.||||||
8799|Isdell Formation|60470|5|Briefly described|p4 Fig. 2, p10-11|Neoproterozoic|Neoproterozoic|in Yeneena Basin, of Throssell Range Group. Shown as part of Lamil Group on p11. Shale, carbonate rocks, and turbidite units||||||
8799|Isdell Formation|62453|4|Described|p5 Fig. 3, 69|Cryogenian|Cryogenian|Geological Province: Paterson Orogen. Of the Lamil Group. Limestone, dolomite, siltstone, shale. Thickness: 1000m+. ||||||
8799|Isdell Formation|64580|4|Described|map legend|Neoproterozoic|Neoproterozoic|Of Lamil Group. Thinly bedded carbonate rock, calcareous siltstone, and minor shale; locally sulfidic.||||||09-DEC-08
8799|Isdell Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic||||||Shale, carbonate rocks, and turbidite units.|
8799|Isdell Formation|64941|5|Briefly described|p27|Tonian|Tonian|Yeneena Basin. Age: 837+/-6 Ma, minimum age for sedimentation, SHRIMP U-Pb zircon, mafic sill at Hasties Reward prospect; and, 858+/-29 Ma pooled Pb-Pb isochron age, interpreted to be timing of diagenesis, carbonates at Telfer.|see comments|Lamil Group||||
8799|Isdell Formation|64943|6|Mentioned|p37|||Stable carbonate shelf||||||
8799|Isdell Formation|65454|4|Described|p7-9, p11, p13, p30 Fig.A1b|Cryogenian|Cryogenian|Yeneena Basin. Of Throssell Range Group. Deep water carbonate with higher silt component in upper parts, which are intruded by dolerite sills. Placed in Lamil Group by Bagas (2004) and Grey et al. (2005). Min age provided by intruded igneous rocks of ~830 Ma. Hosts stratabound Zn-Pb deposits.||||||
8799|Isdell Formation|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Yeneena Basin. Shown as part of Throssell Range Group.||||||23-MAY-16
8799|Isdell Formation|67182|6|Mentioned|p678|Neoproterozoic|Neoproterozoic|Age is from Pb-Pb isochron for carbonate rocks of this Formation (Mass and Huston, unpublished).|ca 860 Ma|||||
8799|Isdell Formation|67202|3|Fully described|p39, p50, p57-59, p61-63, p117|Neoproterozoic|Neoproterozoic|See also p122 Fig.5.9, p128, p155-157, p175-176, p179, p183, p186 Fig.6.14, p187, p190, p192, p203, p208, p238, p245, p280. Yeneena Basin. Over 1km thick. Minimum age from intrusions. Diagenesis dated at 858 +/- 29 Ma (Pb-Pb isochron age; Maas and Huston, unpublished data). Contacts obscured by Cenozoic sediment cover. Gravity and aeromagmetic interpretation. Conductance images. Associated with the Warrabarty Zn-Pb deposit (described), and co-hosts the Telfer Au-Cu deposit (described in detail).|>c.830 Ma.|Topmost Throssell Range Group.||Overlies Broadhurst Formation, unconformably or by tectonic contact. Is overlain by/faulted against the Lamil Group. Is faulted against Coolbro Sandstone.|Carbonate-rich: dark grey, pyritic dolomitic limestone; pale grey to cream dolomite and dolimitic siltstone, shale.|
8799|Isdell Formation|67430|6|Mentioned|p21|||Age of diagenesis.|~860 Ma (Maas and Hudson, unpubl. data).|||||
8799|Isdell Formation|68902|6|Mentioned|p7 fig 4|Neoproterozoic|Mesoproterozoic|Yeneena Basin.||||||
8799|Isdell Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||||||
8799|Isdell Formation|69167|4|Described|geologyp_lut.csv|Neoproterozoic|Neoproterozoic|||Lamil Group|||Thinly bedded carbonate rock, calcareous siltstone, and minor shale; locally sulfidic.|
8799|Isdell Formation|69590|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Neoproterozoic|Geological province: Paterson Orogen. Events: Musgrave Orogeny; Paterson Orogeny. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1000-541 Ma (inferred)||||Thinly bedded carbonate rock, calcareous siltstone, and minor shale; locally sulfidic|
8799|Isdell Formation|71169|6|Mentioned|p8, p10, p16|Neoproterozoic|Neoproterozoic|Yeneena Basin. Pb-Pb carbonate age is interpreted as the timing of diagenesis.|858 +/- 28 Ma (Pb-Pb carbonate, unpublished)|||||
8799|Isdell Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||calcilutite, shale, calcarenite, crystalline carbonate|
8799|Isdell Formation|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Yeneena Basin.|||||Thinly bedded dolomitic limestone, calcareous siltstone, and minor shale; locally sulfidic.|
8821|Jack Hills Group|42579|5|Briefly described|p12|||Variation on "Jack Hills Group". See also Table 2, Fig.3 Jack Hills Greenstone Belt, Plate 1.||||||
8821|Jack Hills Group|46456|14|Not recorded|Not recorded|||||||||
8849|Jameson Range Gabbro|30385|6|Mentioned|p9|||||||||
8849|Jameson Range Gabbro|30389|4|Described|p13|||See also P14||||||
8849|Jameson Range Gabbro|30390|4|Described|p114|||See also p115-128.||||||13-AUG-18
8849|Jameson Range Gabbro|30391|5|Briefly described|p455|||||||||
8849|Jameson Range Gabbro|32692|6|Mentioned|p186|||Unit cell dimensions of olivines||||||
8849|Jameson Range Gabbro|35726|6|Mentioned|p102|||||||||
8849|Jameson Range Gabbro|36551|6|Mentioned|p115|||||||||
8849|Jameson Range Gabbro|36886|3|Fully described|p202|||||||||
8849|Jameson Range Gabbro|44139|5|Briefly described|p284, 285 Fig. 3-69, p286|||Of Giles Complex. 5500m sequence of gabbro, lherzolite, troctolite, anorthosite.| | ||||05-MAR-18
8849|Jameson Range Gabbro|61341|5|Briefly described|Map legend|||Presented in the compound name Jameson Range Troctolite/Gabbro. Intrusion.||||||21-SEP-05
8851|Jamieson Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p222||Early Cretaceous|Pattillo and Nicholls (1990). In figure, Fm = Formation. Thickness: 1400m. Geological Province: Bonaparte Basin. Monotonous succession of silty claystones, with occasional thin limestone or dolomite stringers.  Also on p228 Fig. 18.||||||01-MAR-10
8851|Jamieson Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Early Cretaceous|Browse Basin.||||Overlies Echuca Shoals Formation. Is overlain by Woolaston Formation.||
8851|Jamieson Formation|13267|6|Mentioned|pp277-278.|Early Cretaceous|Early Cretaceous|Contains clays. Acted as a seal for hydrocarbons escaping along faults in Elang and Plover Formations.||||Overlies Darwin Formation.||
8851|Jamieson Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Early Cretaceous|||||Overlies Echuca Shoals Formation. Is overlain by Woolaston Formation.||
8851|Jamieson Formation|13354|6|Mentioned|p375 Fig.6, p385.|Late Cretaceous|Early Cretaceous|Unit of Bathurst Island Group. Overlies Echuca Shoals Formation and underlies Woolaston Formation. Contains shales.||115||||28-OCT-14
8851|Jamieson Formation|23376|4|Described|p229 Fig.2; p244||Albian|Of Bonaparte Basin.||||||28-SEP-06
8851|Jamieson Formation|23378|6|Mentioned|p180 Fig.2||Cretaceous|Of Bathurst Island Group. In the Vulcan Sub-basin.||||||28-SEP-06
8851|Jamieson Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
8851|Jamieson Formation|24207|5|Briefly described|p215, p209 Fig. 5|Aptian|Aptian|Bathyal dark grey to black claystones are typical.  Unconformably overlies the Lower Vulcan Formation.  Max. thickness: 300m (in Londonderry High area).  Geological Province: Vulcan Sub-basin.||||||28-SEP-06
8851|Jamieson Formation|24234|5|Briefly described|p287 Fig.3|Albian|Albian|Overlies Darwin Formation. Geological Province: Bonaparte Basin.||||||
8851|Jamieson Formation|42053|4|Described|p43|||See also Fig.2 p29.||||||01-MAR-10
8851|Jamieson Formation|42056|5|Briefly described|p98|||||||||
8851|Jamieson Formation|42861|6|Mentioned|p4|||||||||
8851|Jamieson Formation|43826|6|Mentioned|Fig.2,p163|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
8851|Jamieson Formation|60385|6|Mentioned|p272 Fig 3, p277|Cenomanian|Aptian|Browse Basin. |||||Mudstone.|
8851|Jamieson Formation|60386|6|Mentioned|p302|Aptian|Barremian|Browse Basin. Distal shelf/basin.||||||
8851|Jamieson Formation|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Late Cretaceous|Early Cretaceous|||Unit in Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Puffin Formation.||
8851|Jamieson Formation|61548|6|Mentioned|p480 Fig.3|Cenomanian|Albian|Northern Bonaparte Basin.||||||
8851|Jamieson Formation|61550|6|Mentioned|p495 Fig.2. |||||Unit in Bathurst Island Group.||Is overlain by Woolaston Formation.||
8851|Jamieson Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Divided into Upper and Lower Jamieson Formation. Age: ~114-~95Ma. Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||01-MAR-10
8851|Jamieson Formation|63358|5|Briefly described|p4 Fig. 1.3|Cenomanian|Aptian|Mentions occur throughout the text. See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
8851|Jamieson Formation|64689|6|Mentioned|p18 Fig.19, p20 Fig.20|||||||Unconformably overlies Echuca Shoals Formation.||
8851|Jamieson Formation|64697|5|Briefly described|p84 Fig.2 |Late Cretaceous|Early Cretaceous|||||||
8851|Jamieson Formation|65078|6|Mentioned|p35|||Contains a clastic "basal transgressive sand" which indicates deltaics and general shallow marine geology. Geological province: Vulcan Sub-basin.||||||30-APR-09
8851|Jamieson Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Cenomanian|Albian|Bathurst Island Group. Underlies the Woolaston Formation, overlies the Echuca Shoals Formation. Mount Ashmore Dome. Deep water claystone.||||||
8851|Jamieson Formation|68223|6|Mentioned|p178-181 Figs. 3 - 6|Cenomanian|Albian|||||||
8851|Jamieson Formation|69297|5|Briefly described|p303, p305, p311|Turonian|Aptian|Barcoo Sub-basin of the Browse Basin. Misspelt as the Jamison Formation on p311.  ||Bathurst Island Group||Overlies the Echuca Shoals Formation. Overlain by the Woolaston Formation.|Mudstones or shales.|
8851|Jamieson Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
8851|Jamieson Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Cenomanian|Albian|See also Sahul: Fig.2. Vulcan: Fig.2-3. Presented also as Upper and Lower Jamieson Formations. May provide a top seal to Vulcan Sub-basin.||Bathurst Island Group.|||Includes claystones and marls.|12-JUL-16
8851|Jamieson Formation|70064|5|Briefly described|Regional p4-8. Central:p2. Northern:p1.|Early Cretaceous|Early Cretaceous|Central Caswell Sub-basin. Contains mixed marine and terrestrial organic matter with moderate to good source potential. Potential regional seal: claystone 500-600m thick across the Sub-basin. Mis-spelt as Jamison in Northern: p1.||||||12-JUL-16
8863|Jandakot Member|41831|4|Described|p556|Pleistocene|Pliocene|Entirely subsurface, richly fossiliferous marine unit.||Yoganup Formation||||04-SEP-14
8863|Jandakot Member|62369|6|Mentioned|p414|Pleistocene|Pliocene|Of the Yoganup Formation. Geological Province: Perth Basin.||||||04-SEP-14
8871|Jap Bay Member|23722|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Parent: Warton Sandstone.   Geological Province: Kimberley Basin||||||07-NOV-08
8871|Jap Bay Member|30533|6|Mentioned|p18|||Occurs in Yampi Sheet area||||||
8871|Jap Bay Member|30897|6|Mentioned|p13|||Stratigraphy||||||
8871|Jap Bay Member|36551|6|Mentioned|p28|||||||||
8871|Jap Bay Member|42814|6|Mentioned|p14|||of Warton Sandstone on Koolan Island||||||
8878|Jarrad Sandstone Member|22496|6|Mentioned|p11||Neoproterozoic|Of the Ranford Formation. geological province: Wolfe Basin.||||||28-SEP-06
8878|Jarrad Sandstone Member|22777|5|Briefly described|Map|||Duerdin Group, Wolfe Basin||||||
8878|Jarrad Sandstone Member|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
8878|Jarrad Sandstone Member|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
8878|Jarrad Sandstone Member|24173|5|Briefly described|p24, p11 Tb.2|Neoproterozoic|Neoproterozoic|Of the Ranford Formation. Conformably overlies Moonlight Valley Tillite;  also overlies, disconformably, the Illjara Sandstone. Geological Province: Wolfe Basin. Max Thickness: 50m. Lithic sandstone.||||||06-APR-05
8878|Jarrad Sandstone Member|28255|5|Briefly described|p76, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of the Ranford Formation (Duerdin Group). Max. thickness: 107m.||||||
8878|Jarrad Sandstone Member|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Briefly described in notes||||||
8878|Jarrad Sandstone Member|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Ranford Formation (Duerdin Group).  Ferruginous sandstone.||||||02-DEC-04
8878|Jarrad Sandstone Member|32701|4|Described|Table 1|||Adelaidean. See p14. Duerdin Gp.||||||28-SEP-06
8878|Jarrad Sandstone Member|32728|6|Mentioned|Table 7|||See also Fig.16||||||
8878|Jarrad Sandstone Member|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Ranford Formation. Fine and medium quartz sandstone; ripple marks and flute casts. Conformable on Moonlight Valley Tillite in north west.||||||27-APR-05
8878|Jarrad Sandstone Member|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Ranford Formation (Duerdin Group). Fine and medium quartz sandstone.||||||27-APR-05
8878|Jarrad Sandstone Member|34230|6|Mentioned|Plate 8|Proterozoic|Proterozoic|Of the Ranford Formation.||||||28-OCT-04
8878|Jarrad Sandstone Member|36888|4|Described|p215|||||||||
8878|Jarrad Sandstone Member|36898|5|Briefly described|Table 1|||||||||
8878|Jarrad Sandstone Member|37927|6|Mentioned|Fig.2|||||||||
8878|Jarrad Sandstone Member|38157|6|Mentioned|Table X|||||||||
8878|Jarrad Sandstone Member|41429|6|Mentioned|p247|||||||||
8878|Jarrad Sandstone Member|43855|5|Briefly described|Map Legend||Proterozoic|||||||
8878|Jarrad Sandstone Member|44140|5|Briefly described|p301 fig 4-7, p302 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. 61 m thick. Shortened to Jarrad Sandstone in Fig.4-7.||Ranford Formation||Overlies Moonlight Valley Tillite. Is overlain by Johnny Cake Shale Member.|Ferruginous dolomitic sandstone; bouldery lenses near base.|07-MAR-18
8878|Jarrad Sandstone Member|44317|4|Described|Table 3, p.7||Adelaidean|||||||
8878|Jarrad Sandstone Member|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
8878|Jarrad Sandstone Member|44324|14|Not recorded|Tb.2.||Adelaidean|Of Ranford Formation.||||||
8878|Jarrad Sandstone Member|44363|5|Briefly described|p.6,14,20|||Member of Ranford Formation. (Adelaidean).||||||28-SEP-06
8878|Jarrad Sandstone Member|44364|14|Not recorded|map legend|||||||||
8878|Jarrad Sandstone Member|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
8878|Jarrad Sandstone Member|45047|2|Defined|p91|Adelaidean|Adelaidean|Described p36.||||||28-SEP-06
8878|Jarrad Sandstone Member|48943|5|Briefly described|p85|||||||||
8878|Jarrad Sandstone Member|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Ranford Formation, Duerdin Group. Ferruginous sandstone.||||||
8878|Jarrad Sandstone Member|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Ranford Formation (Duerdin Group). Geological Province: Wolfe Creek Basin. Dolomitic sandstone and quartz sandstone, siltstone and mudstone.||||||
8878|Jarrad Sandstone Member|60682|4|Described|p17 Table 4, 19|Neoproterozoic|Neoproterozoic|Of Ranford Formation. Conformably overlies Moonlight Valley Tillite. Max. thickness: >50m. Ferrugionus sandstone. Geological Province: Wolfe Creek Basin.||||||03-MAY-05
8878|Jarrad Sandstone Member|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Ranford Formation.||||
8878|Jarrad Sandstone Member|64104|6|Mentioned|p62 fig.1, p71 Tb. 2,  p72 Fig.8, p73|Neoproterozoic|Neoproterozoic|||Unit in Ranford Formation.||Is overlain by Johnny Cake Shale Member.||
8878|Jarrad Sandstone Member|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Ranford Formation, Wolfe Creek Basin. Ferruginous sandstone ||||||
8878|Jarrad Sandstone Member|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Ranford Formation.|||Fine and medium quartz sandstone, locally dolomitic or ferruginous.|
8878|Jarrad Sandstone Member|67484|5|Briefly described|p294-295|Ediacaran|Ediacaran|East Kimberley Region. The 'Member' is omitted in Tb.1. Forms spectacular geological marker in the field.||Of the Ranford Formation.||Overlain by the Johnny Cake Shale. Underlain by the Moonlight Valley Tillite.|Extremely thick massive sandstone with single beds up to 2.5m thick.|
8878|Jarrad Sandstone Member|67620|5|Briefly described|p5 Tbl.1|Ediacaran|Ediacaran|East Kimberley region. The rank (Member) is omitted in the Table.||Ranford Formation.||Overlies Moonlight Valley Formation. Is overlain by Johnny Cake Shale Member.||
8878|Jarrad Sandstone Member|68473|6|Mentioned|p531|||Amadeus Basin.||Ranford Formation||Conformably overlies the Moonlight Valley Formation.||
8878|Jarrad Sandstone Member|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Ranford Formation|||Thin- to thick-bedded, fine-to medium-grained dolomitic sandstone and quartz sandstone, and siltstone and mudstone.|31-JUL-15
8878|Jarrad Sandstone Member|69165|6|Mentioned|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv. ||Ranford Formation|||Thin-thick bedded fine to medium grained dolomitic sandstone and quartz sandstone, siltstone and mudstone.|
8878|Jarrad Sandstone Member|69442|5|Briefly described|p27:3 Tb.27.1, 27:4|||Wolfe Basin. Over 50m thick. Possibly fluvio-glacial deposits (?delta fan). Has a basal cobble conglomerate in WA, some cobbles having glacial striations and chatter-marks.||Ranford Formation.||Conformably overlies Moonlight Valley Tillite (presumably).|Ferruginous sandstone.|12-JUL-16
8878|Jarrad Sandstone Member|69634|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny; King Leopold Orogeny D1/M1.|635-541 Ma (Inferred)|Unit of Ranford Formation.|||Thin- to thick-bedded, fine-to medium-grained dolomitic sandstone and quartz sandstone, and siltstone and mudstone|
8878|Jarrad Sandstone Member|69673|6|Mentioned|p190|||||Ranford Formation||||
8878|Jarrad Sandstone Member|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran||541-635 Ma|Duerdin Group|||thin to thickly bedded, fine to medium grained dolomitic sandstone and quartz sandstone; siltstone and mudstone.|
8878|Jarrad Sandstone Member|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. [previously of Ranford Formation. Ranford Formation not shown in legend]||Duerdin Group|||Ferruginous sandstone.|18-JUL-16
8878|Jarrad Sandstone Member|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Ranford Formation.|||Fine and medium quartz sandstone, locally dolomitic or ferruginous.|
8878|Jarrad Sandstone Member|71267|5|Briefly described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma).|635-541 Ma (inferred)|Unit of Ranford Formation.|||Thin- to thick-bedded, fine-to medium-grained dolomitic sandstone and quartz sandstone, and siltstone and mudstone|
8883|Jasper Gorge Sandstone|14019|4|Described|p16|||Of the Auvergne Group.  Unconformably overlies the Limbunya Group; overlain by the Angalarri Siltstone.  Geological Province: Victoria Basin.  See also p4 Fig. 3.||||||
8883|Jasper Gorge Sandstone|22547|6|Mentioned|Fig4,p25|||Of the Auvergne Group. Geological province: Victoria River Basin. Overlain by Angalarri Siltstone.||||||14-NOV-06
8883|Jasper Gorge Sandstone|24122|3|Fully described|p9, p5 Tb.1|Proterozoic|Proterozoic|Of Auvergne Group.  Conformably overlain by Angalarri Siltstone; unconformably overlies both Bullita and Tijunna Groups (on DELAMERE).  Maximum thickness 100m.  Geological Province: Victoria Basin.||||||
8883|Jasper Gorge Sandstone|24297|3|Fully described|p15|Mesoproterozoic|Mesoproterozoic|Of Auvergene Group. Unconformably overlies Stubb and Wondoan Hill Formations. Now includes some rocks previously included in Wondoan Hill Formation.  See also p5 Tb. 2.||||||
8883|Jasper Gorge Sandstone|24298|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Parent: Auvergne Group. Quartz sandstone/orthoquartzite, minor siltstone and pebbly sandstone.||||||19-OCT-05
8883|Jasper Gorge Sandstone|24300|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Parent: Auvergne Group.   Geological Province: Victoria Basin||||||
8883|Jasper Gorge Sandstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Overlies Stubb Formation; overlain by Angalarri Siltstone. Geological Province: Victoria Basin.||||||08-AUG-05
8883|Jasper Gorge Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Auvergne Group.   Geological Province: Victoria Basin.||||||
8883|Jasper Gorge Sandstone|28255|3|Fully described|p64, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Shallow marine deposit of Auvergne Group. Sandstone; minor siltstone. Conformable over Stubb Fm in northwest area; elsewhere unconformable over Limbunya, Wattie Bullita Gps. Conformable below Angalarri Sst. Max. thickness: 82m. See also p68 Tb.6, p138 App||||||18-OCT-16
8883|Jasper Gorge Sandstone|30003|4|Described|p7, p13|Adelaidean|Adelaidean|Of the Auvergne Group. White and brown flaggy to massive fine to medium quartz sandstone; very minor fissile laminated to thin-bedded light purple and cream micaceous sandstone.||||||19-APR-05
8883|Jasper Gorge Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Adelaidean||||||
8883|Jasper Gorge Sandstone|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
8883|Jasper Gorge Sandstone|32172|4|Described|Table 1|||Adelaidean. Auvergne Group.||||||28-SEP-06
8883|Jasper Gorge Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auverge Group.  Cross-bedded red-brown quartz sandstone, chert fragments near base.||||||16-NOV-04
8883|Jasper Gorge Sandstone|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Massive and blocky medium friable quartz sandstone; minor siltstone, pebbly sandstone.||||||02-DEC-04
8883|Jasper Gorge Sandstone|32307|4|Described|Table 2|||Proterozoic||||||
8883|Jasper Gorge Sandstone|32310|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean/Carpentarian||||||
8883|Jasper Gorge Sandstone|32660|5|Briefly described|Table 6|||||||||
8883|Jasper Gorge Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auverge Group.||||||02-DEC-04
8883|Jasper Gorge Sandstone|32700|3|Fully described|Table 1|||||||||
8883|Jasper Gorge Sandstone|32701|4|Described|Table 1|||See also p9. Adelaidean. Of the Auvergne Group.||||||28-SEP-06
8883|Jasper Gorge Sandstone|32728|6|Mentioned|Fig.14|||||||||
8883|Jasper Gorge Sandstone|32775|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.||||||02-DEC-04
8883|Jasper Gorge Sandstone|33373|3|Fully described|p10|||Table 2.||||||
8883|Jasper Gorge Sandstone|33374|6|Mentioned|p8|||Stratigraphic table.||||||
8883|Jasper Gorge Sandstone|33375|6|Mentioned|p12, p11 Tb. 1|Adelaidean|Adelaidean|Of the Auvergne Group. Blocky medium quartz sandstone; strongly cross-bedded and ripple marked. Max. thickness: 50m.||||||26-APR-05
8883|Jasper Gorge Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
8883|Jasper Gorge Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Auvergne Group.  Medium quartz sandstone.||||||27-APR-05
8883|Jasper Gorge Sandstone|37462|6|Mentioned|Fig.4.13|||||||||
8883|Jasper Gorge Sandstone|45022|6|Mentioned|p.86,87. Tb.12.|||||||||
8883|Jasper Gorge Sandstone|45112|4|Described|p30|||||||||
8883|Jasper Gorge Sandstone|45140|5|Briefly described|p59|||Victoria River region.||Auvergne Group.||Correlated with Wade Creek Sandstone.||
8883|Jasper Gorge Sandstone|48938|2|Defined|p32|Adelaidean|Adelaidean|Measured section pp92,93.||||||28-SEP-06
8883|Jasper Gorge Sandstone|48942|3|Fully described|p61|||Strat. section pp114 and 115.||||||28-SEP-06
8883|Jasper Gorge Sandstone|48943|3|Fully described|p72|||Start. section p137.||||||28-SEP-06
8883|Jasper Gorge Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Victoria Basin. Of Auvergne Group. Overlain by Angalarri Siltstone. Silica cemented sandstone, siltstone and basal conglomerate.||||||23-JUL-04
8883|Jasper Gorge Sandstone|60589|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Auvergne Group.  Silica-cemented sandstone, siltstone, basal conglomerate.  Geological Province: Victoria Basin.||||||26-NOV-04
8883|Jasper Gorge Sandstone|60672|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Medium quartz sandstone, minor siltstone. Of Auvergne Group. Geological Province: Victoria Basin.||||||11-JAN-05
8883|Jasper Gorge Sandstone|60682|4|Described|p8|Cryogenian|Cryogenian|Of Auvergne Group. Unconformably overlies Timber Creek and Skull Creek Formations. Conformably overlain by Angalarri Siltstone. Max. thickness: 130m. Correlated with Ahern Formation. Geological Province: Victoria Basin.||||||
8883|Jasper Gorge Sandstone|60685|4|Described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Predominatly a medium orthoquartzite, rare granular lags. Unconformable on both Stubb and Wondoan Hill Formations; overlain by Angalarri Siltstone. Max. Thickness: 80m. Geological Province: Victoria Basin.||||||19-MAY-05
8883|Jasper Gorge Sandstone|61560|5|Briefly described|p490|Mesoproterozoic|Mesoproterozoic|Of the Auvergne Group. Contains the Matt Wilson impact structure in the Victoria Basin (NT). ||||||
8883|Jasper Gorge Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Auvergne Group, Victoria Basin. Silica cemented sandstone, siltstone, basal conglomerate||||||
8883|Jasper Gorge Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Auvergne Group.||Unconformably overlies Stubb Formation of Tijunna Group. Is overlain by Angalarri Siltstone.||
8883|Jasper Gorge Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Unit in Auvergne Group.||Unconformably overlies Wondoan Hill Formation. Is overlain by Angalarri Siltstone.|Medium quartz sandstone; minor siltstone.|
8883|Jasper Gorge Sandstone|68733|4|Described|p177 Fig.2, p179-183, p185-186, p189-192|Cryogenian|Cryogenian|Victoria Basin. Uniform thickness (~50m) and composition, and is regionally extensive. Forms prominent cliffs in the Victoria River region. Maximum depositional age of ca. 1332 +/- 22 Ma. Deposited in a fluvial to shallow marine environment. Correlated with Heavitree Quartzite (discussed) and Mount Kinahan Sandstone. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1332 +/- 22 Ma.|Basal unit of the Auvergne Group.||Locally unconformably underlain by the Stubb Formation. Conformably overlain by the Angalarri Siltstone.|Characterised by well-sorted red-brown, quartz sandstone with ubiquitous asymmetric ripples.|05-DEC-17
8883|Jasper Gorge Sandstone|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 1.||||Is overlain by Angalarri Siltstone.||12-JUL-16
8883|Jasper Gorge Sandstone|69441|4|Described|p26:1-3|Neoproterozoic|Neoproterozoic|Spectacularly exposed in Jasper Gorge, Gregory National Park. Typically 50-70m thick, up to 130m locally. Near-shore marine on stable, broad continental platform. Conservative maximum deposition age of 1322 +/- 22 Ma, with two isolated grains aged 1243 Ma and 1171 Ma (Carson, 2010).||Auvergne Group.||Unconformably overlies Timber Creek and Skull Creek Formation (Bullita Group). Is overlain conformably by Angalarri Siltstone.|Silica-cemented quartz sandstone, siltstone and basal conglomerate. Mud clasts, now weathered to moulds, are common throughout the lower portion.|12-JUL-16
8883|Jasper Gorge Sandstone|69673|5|Briefly described|p188|||130m thick.|1322 +/- 22 Ma (SHRIMP)|Auvergne Group|||Quartz sandstone with basal conglomerate,|
8883|Jasper Gorge Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group|||Silica cemented sandstone, siltstone and basal conglomerate.|
8883|Jasper Gorge Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Unconformably overlies Timber Creek Formation, Wandoan Hill Formation. Overlain by Angalarri Siltstone.|Medium quartz sandstone; minor siltstone.|21-JAN-22
8883|Jasper Gorge Sandstone|70850|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Unconformably overlies Stubb Formation (Tijunna Group). Is overlain conformably by Angalarri Siltstone.|Silica-cemented sandstone, siltstone, basal conglomerate.|
8883|Jasper Gorge Sandstone|70854|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Victoria Basin.||Auvergne Group.||Unconformably overlies the Wondoan Hill Formation. Unconformably overlain by the Antrim Plateau Volcanics.|Medium quartz sandstone, minor siltstone.|21-SEP-17
8883|Jasper Gorge Sandstone|70855|5|Briefly described|Map legend.|Neoproterozoic|Mesoproterozoic|Victoria Basin.||Auvergne Group.||Locally, unconformably overlies Timber Creek, Skull Creek, Bynoe Formations and Weaner Sandstone (all of the Bullita Group).|Silica-cemented sandstone, siltstone, basal conglomerate.|
8883|Jasper Gorge Sandstone|70968|5|Briefly described|p115-118, p120, p124|Neoproterozoic|Neoproterozoic|Sweet et al. (1974). Victoria Basin. Caps hills and plateaux.||Auvergne Group.||Unconformably overlies Wondoan Hill Formation (Tijunna Group) or Bynoe Formation (Bullita Group).||
8883|Jasper Gorge Sandstone|71080|6|Mentioned|p25|||Basal unit of Victoria Basin. Supersequence 1. Dominated by late Paleoproterozoic detrital zircons||||||
8883|Jasper Gorge Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
8883|Jasper Gorge Sandstone|71302|5|Briefly described|p6,45,72,74|Neoproterozoic|Neoproterozoic|Of Birindudu Basin. Maximum depositional age: 1332+\-26 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Dominated by detritus in the range 1550-1650 Ma, and have very little pre-1800 Ma zircon.||Unit of Auvergne Group.||Overlain by Angalarri Siltstone. Underlain unconformably by Stubb Formation.||
8883|Jasper Gorge Sandstone|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1332+/-22 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
8883|Jasper Gorge Sandstone|71893|5|Briefly described|p69|||This unit has an interpreted maximum depositonal age of 1332 +/- 22 Ma in addition to two younger ages dated at ca 1243 and 1171 Ma (Carson, 2013).||||||
8883|Jasper Gorge Sandstone|73083|6|Mentioned|p18|||||||||
8883|Jasper Gorge Sandstone|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
8896|Jeerinah Formation|22689|6|Mentioned|Fig. 1 p138|||Of Fortescue Group.||||||
8896|Jeerinah Formation|22701|4|Described|p40|Archean|Archean|Fortescue Group, Hamersley Basin. 2684 +/- 6 Ma zircon. Overlies Nymerina Basalt. Overlain by Marra Mamba Formation. Previously Lewin Shale.||||||07-NOV-08
8896|Jeerinah Formation|22837|6|Mentioned|Fig.1 p412|||||||||
8896|Jeerinah Formation|23045|6|Mentioned|287|||||||||
8896|Jeerinah Formation|23046|5|Briefly described|171|||Age 2690-2630 Ma||||||
8896|Jeerinah Formation|23126|5|Briefly described|p382|||||||||
8896|Jeerinah Formation|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Fortescue Group.||||||
8896|Jeerinah Formation|23354|5|Briefly described|315|||||||||
8896|Jeerinah Formation|23570|3|Fully described|p129|Archean|Archean|Of Fortescue Group. Equivalent to some parts of the Lewin Shale.  Overlain by Marra Mamba Iron Formation; underlain by Maddina Formation.   Geological Province: Pilbara Craton||||||07-NOV-08
8896|Jeerinah Formation|23575|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|23583|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group.||||||07-NOV-08
8896|Jeerinah Formation|23594|4|Described|p17|Archean|Archean|Previously Lewin Shale. Of Fortescue Group. Overlying unit Carawine Dolomite. Underlying unit Maddina Basalt. Geological Province: Hamersley Basin. Max. thickness: 250 m.||||||07-NOV-08
8896|Jeerinah Formation|23612|5|Briefly described|p840|Archean|Archean|Of Hardey Formation. Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|23745|4|Described|p12|Archean|Archean|Formerly Lewin Shale. See also page 7 Fig 5. Of Fortescue Group.||||||07-NOV-08
8896|Jeerinah Formation|23746|4|Described|p19|Archean|Archean|Formerly Lewin Shale. Of Fortescue Group. Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|23755|5|Briefly described|p10|||Age: c.2687 Ma. Of Fortescue Group.||||||
8896|Jeerinah Formation|23813|5|Briefly described|p112|Archean|Archean|Shael, tuff, greywacke.  Age: 2687Ma.  Geological Province: Pilbara Craton.  See also p90 Tb. 1||||||07-NOV-08
8896|Jeerinah Formation|23870|5|Briefly described|p224|||Overlies Bunjinah Formation.||||||
8896|Jeerinah Formation|23890|5|Briefly described|p10|Archean|Archean|Of Hamersley Group. Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|23936|4|Described|Tb.1|Archean|Archean|Age: c.2.68-2.67 Ga. Geological Province: Pilbara Craton. Parent: Hamersley Group. Overlying Unit: Marra Mamba Formation. Underlying Unit: Maddina Basalt.||||||07-NOV-08
8896|Jeerinah Formation|24025|5|Briefly described|p14|Archean|Archean|Of Fortescue Group.  Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|24041|5|Briefly described|p493|Archean|Archean|Geological Province: Pilbara Craton||||||07-NOV-08
8896|Jeerinah Formation|24110|5|Briefly described|Plate 1|Archean|Archean|Parent: Fortescue Group.  Geological Province: Hamersley Basin||||||07-NOV-08
8896|Jeerinah Formation|24353|5|Briefly described|p6|Archean|Archean|Of the Fortescue Group. Geological Province: Pilbara Craton||||||07-NOV-08
8896|Jeerinah Formation|24426|6|Mentioned|p220 Fig.5|||||||||07-FEB-11
8896|Jeerinah Formation|24533|5|Briefly described|p5 Table 2, 11|Archean|Archean|Of Fortescue Group. Comprises argillite, sandstone, dolomite, chert and a variety of volcanic rocks. Age: 2684 +/- 6 and 2690 +/- 16Ma. Comformably overlies Maddina Formation, overlain conformably by Marra Mamba Formation.||||||07-NOV-08
8896|Jeerinah Formation|24534|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c. 2686-2629Ma.  Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|24541|3|Fully described|p11 Tb.2, p51-52|Paleoproterozoic|Neoarchean|Of the Fortescue Group. Age: c. 2690-2630 Ma. Conformably overlies the Tumbiana Formation. Maximum Thickness: 200m.||||||07-NOV-08
8896|Jeerinah Formation|24543|5|Briefly described|Map legend|Archean|Archean|Of the Fortescue Group (Mount Bruce Supergroup).  Age: c.2680Ma.  Siltstone and banded chert.||||||07-NOV-08
8896|Jeerinah Formation|24544|4|Described|p57 Fig.43|Archean|Archean|Of Fortescue Group. Overlies Bunjinah Formation. Overlain by Marra Mamba Iron Formation of Hamersley Group. Age: c. 2690-2629 Ma. Tuff and volcanic breccia, basalt. Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|24573|5|Briefly described|p671 Fig.2|||Of the Fortescue Group. Geological Province: Pilbara Craton||||||
8896|Jeerinah Formation|29595|6|Mentioned|Fig.3|||||||||
8896|Jeerinah Formation|29596|6|Mentioned|p1231|||||||||
8896|Jeerinah Formation|29716|4|Described|Table 1|||||||||
8896|Jeerinah Formation|29848|6|Mentioned|p414|||||||||
8896|Jeerinah Formation|30490|6|Mentioned|p112|||||||||
8896|Jeerinah Formation|30766|6|Mentioned|p11|||||||||
8896|Jeerinah Formation|31021|6|Mentioned|Fig. 2|||||||||
8896|Jeerinah Formation|31392|4|Described|p4|||||||||
8896|Jeerinah Formation|31670|4|Described|p911|||||||||
8896|Jeerinah Formation|31671|5|Briefly described|p9|||||||||
8896|Jeerinah Formation|32144|6|Mentioned|p116|||Solvent extractable organic matter||||||
8896|Jeerinah Formation|32389|4|Described|p925|||||||||
8896|Jeerinah Formation|33538|6|Mentioned|p288|||||||||
8896|Jeerinah Formation|33542|6|Mentioned|p411|||||||||
8896|Jeerinah Formation|33544|6|Mentioned|p40|||See also PP82, 150, 281 & Plate 4||||||
8896|Jeerinah Formation|33687|5|Briefly described|p916|||||||||
8896|Jeerinah Formation|34066|4|Described|p5|||L.Prot.||||||
8896|Jeerinah Formation|34128|6|Mentioned|p17|||Proterozoic||||||
8896|Jeerinah Formation|34129|6|Mentioned|p57|||Proterozoic||||||
8896|Jeerinah Formation|34135|4|Described|Table 1|||See also Table 2, PP10,11,17. Lower Proterozoic.||||||
8896|Jeerinah Formation|35059|6|Mentioned|p205|||||||||
8896|Jeerinah Formation|35218|4|Described|p4|||||||||
8896|Jeerinah Formation|35260|5|Briefly described|Table 1|||||||||
8896|Jeerinah Formation|35269|6|Mentioned|p304|||||||||
8896|Jeerinah Formation|35299|6|Mentioned|Fig.2|||||||||
8896|Jeerinah Formation|36091|5|Briefly described|p572|||||||||
8896|Jeerinah Formation|36551|6|Mentioned|p22|||See also Table 23.||||||
8896|Jeerinah Formation|36882|4|Described|p127|||||||||
8896|Jeerinah Formation|37297|6|Mentioned|p93|||||||||
8896|Jeerinah Formation|37327|6|Mentioned|p393|||||||||
8896|Jeerinah Formation|37460|3|Fully described|Table 3.I|||Also described Table 3.III||||||
8896|Jeerinah Formation|37704|6|Mentioned|p507|||||||||
8896|Jeerinah Formation|38790|6|Mentioned|Table 1|||||||||
8896|Jeerinah Formation|39030|5|Briefly described|p3|||||||||
8896|Jeerinah Formation|39200|6|Mentioned|p279|||||||||
8896|Jeerinah Formation|39210|5|Briefly described|Table 1|||||||||
8896|Jeerinah Formation|39424|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
8896|Jeerinah Formation|39426|6|Mentioned|p11|||||||||
8896|Jeerinah Formation|39697|3|Fully described|p123|||||||||
8896|Jeerinah Formation|39837|6|Mentioned|Table 1|||||||||
8896|Jeerinah Formation|40369|6|Mentioned|Table 1|||||||||
8896|Jeerinah Formation|40904|6|Mentioned|p85|||||||||
8896|Jeerinah Formation|41357|6|Mentioned|Fig.2|||||||||
8896|Jeerinah Formation|41635|6|Mentioned|Table 2|||||||||
8896|Jeerinah Formation|41669|4|Described|p25|||||||||
8896|Jeerinah Formation|41768|4|Described|p26|||See also Table 1||||||
8896|Jeerinah Formation|42013|5|Briefly described|Map Legend|Archean||||||||07-NOV-08
8896|Jeerinah Formation|42112|4|Described|p7|||||||||
8896|Jeerinah Formation|42148|6|Mentioned|p690|||||||||
8896|Jeerinah Formation|42190|5|Briefly described|p274|||||||||
8896|Jeerinah Formation|42260|5|Briefly described|p127|||||||||
8896|Jeerinah Formation|42352|5|Briefly described|p5, Fig.3 p6, p14|||Part equivalent to Lewin Shale of Hickman (1978)||||||
8896|Jeerinah Formation|42471|4|Described|p6|||||||||
8896|Jeerinah Formation|42472|5|Briefly described|Map legend|||||||||
8896|Jeerinah Formation|42686|5|Briefly described|map legend|Archean||||||||07-NOV-08
8896|Jeerinah Formation|42704|5|Briefly described|Plate 1 and Plate 2E|Archean||Of the Fortescue Group. Mudstone, siltstone, chert, sandstone, dolerite, felsic tuff, pillowed metabasalt. Intruded by metadolerite sills.||||||07-NOV-08
8896|Jeerinah Formation|42743|5|Briefly described|map legend|Archean||||||||07-NOV-08
8896|Jeerinah Formation|42744|4|Described|p4|||||||||
8896|Jeerinah Formation|42785|5|Briefly described|p262, p269|||see also Fig.3 P264||||||
8896|Jeerinah Formation|42898|5|Briefly described|p339, Fig.2 p341|||of Fortescue Group||||||
8896|Jeerinah Formation|43037|5|Briefly described|p25|||of Fortescue Group||||||
8896|Jeerinah Formation|43052|5|Briefly described|p49|||of Fortescue Group||||||
8896|Jeerinah Formation|43055|4|Described|p16, Table 4|||of Fortescue Group||||||
8896|Jeerinah Formation|43056|5|Briefly described|Map Legend|||of Fortescue Group||||||
8896|Jeerinah Formation|43063|6|Mentioned|p47|||of Fortescue Group||||||
8896|Jeerinah Formation|43119|4|Described|p7|||of Fortescue Group||||||
8896|Jeerinah Formation|43210|5|Briefly described|Table1 p3,p4.||Archean|of Fortescue Group.||||||07-NOV-08
8896|Jeerinah Formation|43262|5|Briefly described|Map Legend||Archean|Of the Fortescue Group.||||||07-NOV-08
8896|Jeerinah Formation|43290|3|Fully described|p5||Archean|Of the Fortescue Group.||||||07-NOV-08
8896|Jeerinah Formation|43595|5|Briefly described|Table 2-29,p219|||||||||
8896|Jeerinah Formation|44151|6|Mentioned|p158|||||||||
8896|Jeerinah Formation|44152|5|Briefly described|p173-174, p176 Fig.2-154|||Defined by de la Hunty (1965) as topmost unit in Fortescue Group. Divided into 3 Members by MacLeod and de la Hunty (1966).||Fortescue Group|Warrie Member, Roy Hill Shale Member, Woodiana Sandstone Member; Nallanaring Volcanic Member|||
8896|Jeerinah Formation|44189|5|Briefly described|Map legend||Archean|||||||07-NOV-08
8896|Jeerinah Formation|44190|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8896|Jeerinah Formation|44229|5|Briefly described|Map Legend|Archean|Archean|Of the Fortescue Group.  Shale, siltstone, sandstone, and reworked pisolitic lapilli and vtric-crystal tuff.  Age: c.2687Ma.||||||07-NOV-08
8896|Jeerinah Formation|44438|14|Not recorded|map legend||Paleoproterozoic|Fortescue Group of Mt. Bruce Supergroup. L.Proterozoic.||||||07-NOV-08
8896|Jeerinah Formation|44443|6|Mentioned|map legend|Paleoproterozoic|Paleoproterozoic|Of Fortescue Group. Correlated with Lewin Shale.||||||07-NOV-08
8896|Jeerinah Formation|44477|4|Described|p.10-11, Table 1||Proterozoic|SF/50-6.||||||
8896|Jeerinah Formation|44478|14|Not recorded|map legend||Proterozoic|||||||
8896|Jeerinah Formation|44481|5|Briefly described|map legend||Paleoproterozoic|||||||07-NOV-08
8896|Jeerinah Formation|44501|4|Described|p.6,11,,13,16,17,18||Proterozoic|See also p.30 table 4, for more details. (ref. to MacLeod et al 1963). (F/50-7).||||||
8896|Jeerinah Formation|44502|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
8896|Jeerinah Formation|44503|2|Defined|p.7,9,11,18,tb.2,map|||Contains Roy Hill Shale, Warrie, Woodiana Sandstone Members. Roy Hill Sheet. (F50-12).||||||
8896|Jeerinah Formation|44504|14|Not recorded|map legend||Proterozoic|||||||
8896|Jeerinah Formation|44692|2|Defined|p.7,10,11,26,Tb.1|||(F50-11).||||||
8896|Jeerinah Formation|44729|5|Briefly described|map legend|Proterozoic||Of Fortescue Group||||||
8896|Jeerinah Formation|44831|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
8896|Jeerinah Formation|46319|6|Mentioned|p14|||||||||
8896|Jeerinah Formation|50131|6|Mentioned|p6 Fig. 4|||Of Fortescue Group. Geological Province: Pilbara Craton.||||||22-APR-09
8896|Jeerinah Formation|50189|4|Described|arch|Archean|Archean|Of the Fortescue Group. Disconformably overlies the Maddina Formation. Basal brown tuffaceous siltstone, khaki brown lapilli tuff, and siliceous vitric and crystal lithic tuffs - overlain by siltstone, wacke, conglomerate and chert. Max. Thickness: >300m.||||||07-NOV-08
8896|Jeerinah Formation|50227|5|Briefly described|p443 Fig. 1|Archean|Archean|Age: 2690Ma.||||||07-FEB-11
8896|Jeerinah Formation|50287|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Age: c. 2687 Ma. Geological Province: Hamersley Basin. Thin-bedded chert, silicified shale, and mudstone; minor sandstone.||||||07-NOV-08
8896|Jeerinah Formation|50382|5|Briefly described|Map Legend|Archean|Archean|Of Fortescue Group. Geological Province: Hamersley Basin, Pilbara Craton. Age: c. 2680 Ma||||||07-NOV-08
8896|Jeerinah Formation|50544|3|Fully described|p50, p15 Tb. 1|Archean|Archean|Top of the Fortescue Group.  Originally mapped as Lewin Shale (de la Hunty, 1966; Hickman et al, 1983).  Includes the locally thick igneous Maramine Volcanic and Isabella Members.  Age: c.2684Ma.  Max. thickness: 700m.  Geol. Province: Hamersley Basin.||||||23-DEC-09
8896|Jeerinah Formation|50555|5|Briefly described|Map legend|Archean|Archean|Of the Fortesque Group (Mount Bruce Supergroup).  Includes Isabella, Baramine Volcanic and Kuruna Mbrs.  Mixed sedimentary rocks.  Overlies Maddina Fm.; underlies Carawine Dolomite.  Age: c.2687Ma.  Geol.Prov: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|60373|4|Described|p145 Tb. 1, p147 Fig. 2, p150 Tb. 2|Archean|Archean|Of Fortescue Group. Includes Roy Hill Shale, Warrie and Woodiana Sandstone Members. Overlain by Marra Mamba Iron Formation, underlain by Maddina Formation. Age: 2629+/-5, 2684+/-6, 2690+/-16Ma (SHRIMP).||||||01-JUL-14
8896|Jeerinah Formation|60429|5|Briefly described|p20 Fig. 5, p21, p23|Archean|Archean|Of the Fortescue Group. Previously mapped as Lewin Shale. Disconformably overlies Maddina Formation.||||||07-FEB-11
8896|Jeerinah Formation|60635|6|Mentioned|p51 Fig. 2.2A|||||||||
8896|Jeerinah Formation|60706|5|Briefly described|p623 Fig.2, p644 App.1|Archean|Archean|Of the Fortescue Group. Includes the Roy Hill Shale Member. Age: 2629+/-5 Ma (SHRIMP). Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|61254|6|Mentioned|p258 Fig.2.|Neoarchean|Neoarchean||ca. 2685 Ma|Unit in Fortescue Group.|Includes Woodiana Sandstone Member and Roy Hill Shale Member.|Overlies Maddina Formation.||
8896|Jeerinah Formation|61265|5|Briefly described|p46-47 Fig.2, p51 Tb.2|Archean|Archean|Age: 2684+/-6 Ma (Arndt et al. 1991). Geological Province: Pilbara Craton.||||||07-NOV-08
8896|Jeerinah Formation|61268|5|Briefly described|p79, p81 Tb.1|||Of the Fortescue Group. Mudstone, siltstone, sandstone, chert and basaltic lavas and breccia; minor felsic volcaniclastic rock. See also p80 Fig.2, p83 Fig.4.||||||
8896|Jeerinah Formation|61560|5|Briefly described|p498 Tb. 4|Archean|Archean|Displays impact spherules caused by impact ejecta. Age: 2.63Ga. Geological Province: Hamersley Basin. See also p500, p501.||||||07-NOV-08
8896|Jeerinah Formation|61575|5|Briefly described|p759|Neoarchean|Neoarchean|Lowest unit of the Fortescue Group. Unconformably overlain by the Carawine Dolomite (Hamersley Group). Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|61576|5|Briefly described|p774 Fig. 1||Neoarchean|Of the Fortescue Group. Age: 2687Ma. Geological Province: Hamersley Basin.||||||07-NOV-08
8896|Jeerinah Formation|61577|5|Briefly described|p787 Tb. 1|Archean|Archean|Of the Fortescue Group. Underlies Marra Mamba Iron Formation.  Age: >2.63Ga. Geological Province: Pilbara Craton.||||||07-NOV-08
8896|Jeerinah Formation|62129|3|Fully described|p6, p8, p20, p21, p25|Archaean|Archaean|Of Fortescue Group. Conformably underlain by Bunjinah Formation and Maddina Basalt, conformably overlian by Marra Mamba Iron Formation. Thickness: 1800m. Geological Province: Hamersley Basin.||||||07-FEB-11
8896|Jeerinah Formation|62130|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Includes Woodiana Member. Geological Province: Hamersley Basin, Pilbara Craton. Pelite, metasandstone, chert, metabasaltic pillow lava and breccia, and metamorphosed felsic volcanic rock; intruded by metadolerite sills.||||||23-MAR-09
8896|Jeerinah Formation|62576|5|Briefly described|p619|Archean|Archean|Of the Fortescue Group. Overlies Maddina Formation. Age: 2630Ma. Geological province: Pilbara Craton. Includes shales. ||||||07-NOV-08
8896|Jeerinah Formation|62579|5|Briefly described|p116|Archean|Archean|Topmost unit of Fortescue Gp (Mount Bruce Supergp). Includes Woodiana and Warrie Members +Roy Hill Shale. Age: 2629+/-5Ma. Geol.Prov: Pilbara Craton. Mostly of volcaniclastic rock, volcaniclastic sandstone, stromatolitic carbonate, chert, basalt and tuff.||||||07-NOV-08
8896|Jeerinah Formation|63153|5|Briefly described|p1359, p1363, p1372. |||Chert pods are common.||Of the Fortescue Group.|Includes Roy Hill Shale.|Is overlain conformably by Marra Mamba Iron Formation (Hamersley Group).||
8896|Jeerinah Formation|63367|5|Briefly described|p230-236, p244-246|Neoarchean|Neoarchean|Trace elements and REE + Y data discussed in detail.|ca. 2.70 Ga|Topmost unit in Fortescue Group.|||Mudrock; includes carbonate rocks.|
8896|Jeerinah Formation|63372|4|Described|Map Legend|Archean|Archean|Of the Fortescue Group. Geological Province: Hamersley Basin. Age: 2690-2629Ma. Shale, siltstone, mudstone, chert, and local dolomite and sandstone. Overlies: Maddina Formation.||||||07-NOV-08
8896|Jeerinah Formation|63417|5|Briefly described|Map legend|Archean|Archean|Of Fortescue Group (Mount Bruce Supergroup). Age: 2690-2629Ma. Geological Province: Fortescue Basin. Siliciclastic sedimentary rocks; local volcanic rocks and dolerite sills.||||||07-NOV-08
8896|Jeerinah Formation|63432|5|Briefly described|p735 Fig. 1, p736 Fig. 2|Archean|Archean|Of the Fortescue Group. Geological Province: Pilbara Craton.||||||07-FEB-11
8896|Jeerinah Formation|64384|4|Described|p25, p29 Tb.5, p34-5||Archean|Of Fortescue Gp.Overlain by cherty iron formation, then Carawine Dolomite. Thickness: >900m. Geol.prov: northen Pilbara Craton/southern Hamersley Basin. Siltstone; shale and chert; sst, local felsic lava, tuff+agglom; basalt; mafic sills locally abundant||||||07-FEB-11
8896|Jeerinah Formation|64580|4|Described|map legend||Neoarchean|Of Fortescue Group.Mudstone; siltstone; sandstone; chert; massive basaltic flows; basaltic pillow lava; basaltic breccia; and minor felsic volcaniclastic rock; intruded by numerous dolerite sills; metamorphosed.||||||09-DEC-08
8896|Jeerinah Formation|64654|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2690-2629Ma. Geological Province: Pilbara Craton (Hamersley Basin). Shale, chert, siltstone, fine-grained sandstone.||||||
8896|Jeerinah Formation|64656|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2690-2629Ma. Geological Province: Hamersley Basin.||||||26-NOV-08
8896|Jeerinah Formation|64657|5|Briefly described|Map Legend|Archaean|Archaean|Of Fortescue Group. Age: 2690-2629Ma. Geological Province: Hamersley Basin. Shale, siltstone and minor shale.||||||
8896|Jeerinah Formation|64724|4|Described|p43, p42 Fig. 3|Neoarchean|Neoarchean|Basalt erupted during extension of the Hamersley Basin. Overlain by Hamersley Group rocks.||Of Fortescue Group.||||02-APR-12
8896|Jeerinah Formation|65683|5|Briefly described|p799, p801 Fig2, p803, p805|||Of Fortescue Group. Includes Roy Hill Shale Member.||||||08-MAR-12
8896|Jeerinah Formation|65724|5|Briefly described|map legend|Neoarchaean|Neoarchaean|Of Fortescue Group. Includes Baramine Member. Unconf. under Paterson Fm; under Carawine Dolomite; over Maddina Fm. Shale, chert and dolomite. Age: 2690-2629 Ma (geochron: NT Arndt etal 1991; DR Nelson etal 1999). Geol.Prov: Hamersley Basin, Pilbara Craton||||||
8896|Jeerinah Formation|65757|5|Briefly described|p81 Tb.2|Neoarchean|Neoarchean|Part of the Fortescue Group. Overlain by Marra Mamba Iron Formation. Carbonate-chlorite spherules in breccia. Age: 2629+/-5 Ma. Shown as Jeerinah Shale p85.||||||
8896|Jeerinah Formation|65825|4|Described|p7 Fig.4,  p20, p23. |Archean|Archean|Formerly Lewin Shale (de la Hunty 1964). Typically forms a resistant cap over deeply weathered shale and siltstone, forming prominent hills.  A large dolerite sill intrudes along the contact with Maddina Formation.|2690 to 2629 Ma (Arndt et al. 1991).|Unit in Fortescue Group.|||Fine-grained clastic sedimentary rocks: siltstone, shale, minor medium- to coarse-grained sandstone; minor thin to thick bedded, grey to pale green-grey chert with a vague lamination.|
8896|Jeerinah Formation|65827|6|Mentioned|p39|Neoarchean|Neoarchean|Overlies Maddina Formation.||||||21-JAN-22
8896|Jeerinah Formation|65828|5|Briefly described|Map legend|Archean|Archean||c.2687 Ma (Arndt et al. 1991).|Unit in Fortescue Group.||Overlies Maddina Formation.|Thin-bedded chert, silicified shale, and mudstone; minor sandstone.|
8896|Jeerinah Formation|65829|3|Fully described|p4, p7 Fig.3, p10, p15, pp21-22, p32.|Neoarchean|Neoarchean|Named by MacLeod et al. (1963).  Shale, chert and dolomite units mapped as Lewin Shale by Hickman (1978) were later assigned to this Formationt by Hickman (1983). Marine sediments and mafic volcanics, intruded by thick, coarse-grained dolerite sills. Over 500 m thick. Local occurrences of partly silicified sheets of dissected, secondary carbonate or residual calcrete. Part of Mount Jope Supersequence (Blake et al. 2004).|2690 - 2629 Ma.|Uppermost unit in Fortescue Group.|Includes Baramine and Roy Hill Shale Members.|Overlies disconformably, or is faulted against, the underlying Maddina Formation. Is overlain disconformably, or is faulted against, the Carawine Dolomite.|Basal red-brown weathering, fine-grained quartz sandstone; blue-grey limestone; dark grey siltstone and shale; coloured and banded cherts, dolomite, local stromatolitic limestone; black and grey carbonaceous and pyritiferous shale.|
8896|Jeerinah Formation|66217|5|Briefly described|p45.|||Fortescue Basin.||Uppermost unit in Fortescue Group.|||Mainly argillaceous rocks in the north; basaltic lava and volcaniclastic rocks in the south.|
8896|Jeerinah Formation|66685|5|Briefly described|p217 Fig.2|Archean|Archean|First generally recognized marine transgression within the Fortescue Group, marking the establishment of a passive margin (Barley et al. 1998) and the end of terrestrial deposition (Blake et al 2004). |<2715 Ma.|Fortescue Group|Woodiana, Warrie, Roy Hill Members.|Overlies the Maddina Formation.|Includes basalt, sandstone and stromatolites.|
8896|Jeerinah Formation|66882|5|Briefly described|p118|Neoarchean|Neoarchean|Detrital zircons of the same age occur in Cook Gap Schist, Gawler Craton.|2690+/-16 Ma|Hamersley Group.|||Tuffaceous sandstone.|
8896|Jeerinah Formation|66887|5|Briefly described|p21 Fig.11|||Pilbara Craton.||Fortescue Group||||14-DEC-16
8896|Jeerinah Formation|67025|5|Briefly described|p319 Fig.2, p322 Table 3, pp324-325.|Archean|Archean|||Topmost unit in Fortescue Group.||Conformably overlies Mount Jope Volcanics. Is overlain conformably by Marra Mamba Iron Formation of the Hamersley Group.||
8896|Jeerinah Formation|67056|6|Mentioned|p442 Fig.14.|||Actually shown as Jeerinah Shale, overlain by Marra Mamba Iron Formation.||||||06-AUG-15
8896|Jeerinah Formation|67130|5|Briefly described|p3 fig 2, p34 fig 29, p39 fig 36|Neoarchean|Neoarchean||2690 Ma - 2629 Ma|Fortescue Group||Overlies Maddina Basalt, Mount Jope Volcanics, overlain by Marra Mamba Iron Formation|Shale.|
8896|Jeerinah Formation|67183|4|Described|p643, 645, p649-52, 657, 659, 661, 665 |Archean|Archean|Previously known as the Lewin Shale. In the Woodie Woodie mine corridor a syn-sedimentary fault breccia is present in the uppermost shale horizons, clearly disrupting chert and shale units, but conformably overlain by shale.|2684 Ma|Fortescue Group, Mount Bruce Supergroup||Conformably overlies the Maddina Formation; gradationally (conformably) underlies the Marra Mamba Iron Formation (in the southeast Pilbara) and the Carawine Dolomite.|Consists of shale, chert, siltstone with minor sandstone, dolomite, conglomerate and localised fault breccia. Interbedded shale, dolomite and chert.|
8896|Jeerinah Formation|67201|4|Described|p28-30, p32, p34 Fig.18, p36, p51-54|||In northern Pilbara Craton, Fortescue Basin. Boundary with underlying Maddina Formation does mark a significant change from volcanism to predominantly sedimentary deposition. Thickness: ~150 m in central and eastern Pilbara; 1-2 km thick in southern Pilbara ranges. 2710-2630 Ma. Lower nearshore shelf deposits and upper section of 'deeper' offshore shelf facies (central and eastern Pilbara). In contrast (southern Pilbara ranges), laterally variable assemblage of 'deeper' shelf deposits. Occurrence of extensive metadolerite sills restricted to S-SW side of Jeerinah-Sylvania Fault Zone.|c.2690-c.2629 Ma SHRIMP U-Pb Trendall et al. 2004|Top of Fortescue Group|Roy Hill Member, Warrie Member, Woodiana Member, Nallanaring Member|Overlain by Brockman Island Formation (Hamersley Group). Woodiana Member (Jeerinah Formation) conformably overlies Maddina Formation.|Massive basaltic lava, pillow lava, hyaloclastite, argillite, chert, dolomite, and sandstone; shale, chert and BIF; felsic volcaniclastics. Metamorphosed. Predominantly phyllite. Up to 60% mafic sills.|
8896|Jeerinah Formation|67202|4|Described|p51-52, p119-120, p124-p125, p258,|Archean|Archean|Fortescue Basin. See also p280-281. Thickness c. 350m. Conductivity described and imaged.||Fortescue Group.||Overlies Maddina Formation. Is overlain disconformably by Carawine Dolomite. Faulted against the Tarcunyah Group.|Mixed volcaniclastic and epiclastic succession of tuffaceous siltstone, lapilli tuff, wacke, conglomerate and chert. Elsewhere described as a shale-rich unit with intercalated chert, dolomite and basalt.|15-FEB-18
8896|Jeerinah Formation|67229|6|Mentioned|p3 Fig.2|||MacLeod and de la Hunty (1965). Previously the lower part of the Lewin Shale of de la Hunty (1964). Williams (1968) added the Nallanaring Volcanic Member to the original three Members.|||Woodiana Sandstone, Warrie, Roy Hill Shale, Nallanaring Volcanic, Members.|||
8896|Jeerinah Formation|67721|5|Briefly described|p37|Neoarchean|Neoarchean|Geochronology from tuffaceous sandstones.|2690 +/- 16 Ma (Arndt et al. 1991)|||||
8896|Jeerinah Formation|67855|6|Mentioned|p225, 226|||Hamersley Basin.||||||
8896|Jeerinah Formation|68035|4|Described|p291, 292, Fig 6, 293|Neoarchean|Neoarchean|Fortescue Basin. Is much thicker  in S than in the N, and consists of 'deeper' shelf deposits, including basalt, as well as being extensively intruded by dolerite sills. Stromatolites also occur in shallow-water chert at the base. |2690 - 2629 Ma|Top of Fortescue Group.||Overlies Maddina Formation. Overlain by Marra Mamba Iron Formation, Hamersley Group.|Basal near-shore facies of sandstone and stromatolitic limestone overlain by an off-shore facies of mudstone, carbonate rocks, carbonaceous pyritic shale, and chert.|
8896|Jeerinah Formation|68056|5|Briefly described|p170-172, 176-177, 183-188, 190|Archean|Archean|Pilbara Craton. Fe, C isotope data and pyrite shapes tabulated. Age range is also given as c.2715 to 2630 Ma.|2684 +/- 6 Ma.||Woodiana Sandstone, Roy Hill Shale, Warrie, Members.|Unconformably overlies Maddina Formation. Is overlain conformably by Marra Mamba Iron Formation.|Fining-upwards sequence: conglomerate, siliceous mudstone, quartzite and shale.|
8896|Jeerinah Formation|68101|6|Mentioned|p1, p6|||||Fortescue Group||||
8896|Jeerinah Formation|68280|5|Briefly described|p5, p54, p62|Neoarchean|Neoarchean||2690-2629 Ma|Fortescue Group||Overlain by Marra Mamba Iron Formation, overlies Maddina Formation|Shale.|
8896|Jeerinah Formation|69028|5|Briefly described|Map Legend|Neoarchean|Neoarchean|Fortescue Basin. Includes an unnamed unit of metamorphosed pillowed and massive basaltic flows and basaltic breccia.||Of the Fortescue Group.|||Undivided mudstone, siltstone, sandstone, and chert; massive basaltic flows, basaltic pillow lava, basaltic breccia; minor felsic volcaniclastic rock; intruded by numerous dolerite sills; metamorphosed.|06-MAY-14
8896|Jeerinah Formation|69080|5|Briefly described|p687, p693|Neoarchean|Neoarchean|||Topmost unit in Fortescue Group.||Overlies Bunjinah Formation. Is overlain conformably by Marra Mamba Iron Formation (Hamersley Group).||
8896|Jeerinah Formation|69166|5|Briefly described|500k_geologyp08_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|||Pillowed and massive basaltic flows, basaltic breccia. Mudstone, siltstone, sandstone, chert, minor felsic volcanics intruded by dolerite sills.|
8896|Jeerinah Formation|69167|4|Described|geologyp_lut.csv|Neoarchean|Neoarchean|||Fortescue Group|Includes Isabella Member, Baramine Member||Thin-bedded chert, silicified shale, shale, siltstone, mudstone, dolomite and  sandstone. Siliciclastic sedimentary rocks, local volcanic rocks (basalt), dolerite sills, minor carbonate rocks and basaltic volcanic rocks.|
8896|Jeerinah Formation|69185|4|Described|GEOL_LUT_CSV files||Neoarchean|Geological Province: Pilbara Craton. Of Northwest, Northeast, and South Pilbara Sub-basins, Hamersley Basin. See 500k_geologyp08_lut.csv, 500k_interpgeop_pilcrat02_lut.csv.|c. 2680 Ma|Unit of Fortescue Group.|||Undivided; mudstone; siltstone; sandstone; chert; massive basaltic flows; basaltic pillow lava; basaltic breccia; and minor felsic volcaniclastic rock; intruded by numerous dolerite sills; metamorphosed|
8896|Jeerinah Formation|69299|4|Described|p7, p19|Neoarchean|Neoarchean|Top of Fortescue Group. Not preserved on COOYA POOYA. Age from Nallanaring Volcanic Member sample obtained 75 km west of COOYA POOYA.|2684 +/- 6 Ma (Arndt et al. 1991).|Of Fortescue Group.|Includes Nallanaring Volcanic Member.|Overlies Maddina Formation.|Dominantly sedimentary.|01-JUL-14
8896|Jeerinah Formation|69301|4|Described|p16-19, p22-23|||Pilbara Craton. Fortescue Basin. Northeast Pilbara Sub-basin, Northwest Pilbara Sub-basin, South Pilbara Sub-basin, Sequence 4. |2.69-2.63 Ga|Stratigraphically highest in Fortescue Group|Roy Hill Member, Warrie Member, Woodiana Member, Nallanaring Member||Mainly composed of shale, chert, and BIF. Clastic succession. Predominantly marine sedimentary rocks. Stromatolites.|
8896|Jeerinah Formation|69538|5|Briefly described|p532 Tb.3, p572-573, p583-585|Paleoproterozoic|Paleoproterozoic|Basement in Chichester Range area of Fortescue Valley.||Unit in Fortescue Group.||||
8896|Jeerinah Formation|69563|5|Briefly described|p690-691, p693, p695 Fig.5, p697|||U-Pb zircon ages: maximum from Arndt et al. (1991); minimum from Nelson et al. (1999).|2684 +/- 6 Ma - 2629 +/- 5 Ma.|Unit in Fortescue Group.|Includes Roy Hill Member.||A sequence of siltstone, chert, carbonate rocks and mafic volcanics.|25-MAY-16
8896|Jeerinah Formation|69569|6|Mentioned|p285 Fig.1|||East Pilbara Terrane.||Fortescue Group.||||
8896|Jeerinah Formation|69590|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Of Fortescue Basin. Events: Capricorn Orogeny; Edmundian Orogeny; Ophthalmian Orogeny; Pilbara Craton breakup. See 100k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|2715-2629 Ma (inferred)|Unit of Fortescue Group.|Includes Baramine Volcanic Member, Isabella Member.||Basalt and dolerite, mixed sedimentary rocks; shale, siltstone, sandstone, and local microbanded chert; accretionary lapilli; minor carbonate rock; thin bedded-dolomite.|
8896|Jeerinah Formation|69739|6|Mentioned|p70 Fig.3|||Hamersley Basin.||Fortescue Group.||Is overlain by Marra Mamba Iron Formation.||
8896|Jeerinah Formation|69745|6|Mentioned|p272-273, 287|||Mount Wall area, Hamersley Province.||Fortescue Group.|||Carbonaceous shales, chert and siltstone. Locally (Mount Wall region) heavily intruded by dolerite sills.|
8896|Jeerinah Formation|69792|6|Mentioned|p1095-7, p1107|||Minimum age shown as c. 2630 Ma.||Unit in Fortescue Group.||||22-JUN-20
8896|Jeerinah Formation|70795|6|Mentioned|2_5m_interpgeop15_lut.csv|Neoarchean|Neoarchean|Also 500k_interpgeop14_lut.csv|2715-2629 Ma|Fortescue Group||||
8896|Jeerinah Formation|71042|4|Described|p64 fig 1, p66, p69-p72|Archean|Archean|Oakover Basin. See also  p74, p76-p77, p79-p82, p86, p89-p90, p94-p96.||Fortescue Group||Conformably overlain by the Carawine Dolomite and Googhenama Formation. Overlies the Maddina Formation.|Shale and chert.|
8896|Jeerinah Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, mudstone, crystalline dolostone/dolomite, shale|
8896|Jeerinah Formation|71550|6|Mentioned|p45|||Geological province: Of Hamersley Basin. Possible source of c. 2.68 Ga zircons in the Turee Creek Group and Beasley River Quartzite.||Unit of Fortescue Group.||||03-SEP-19
8896|Jeerinah Formation|71803|4|Described|p365-p368, p371, p375, p380|Neoarchean|Neoarchean|Pilbara Craton. An additional age of 2684 +/- 6 Ma is derived from Arndt et al, 1991.|2690 +/- 16 Ma (Arndt et al, 1991)|Fortescue Group|||Sedimentary rocks including clastic, carbonate and cherts and subaqueous mafic lavas and volcaniclastic rocks.|
8896|Jeerinah Formation|71808|4|Described|vi, ix, p8-p9, p45-p46|Neoarchean|Neoarchean|Hamersley Province. Intruded by extensive dolerite sills. In the study area this unit is the only representative of the Fortescue Group and occurs in the cores of Weeli Wolli, Alligator and Wonmunna Anticlines to the core of the Milli Milli Dome and the south side of Parallel Ridge. Historically subdivided into three regional members; the upper Roy Hill Shale, central Warrie Shale and lower Woodiana Sandstone Members. Thorne and Trendall (2001) no longer recognise the division of the two shale members and simplifyy the Roy Hill Shale to the Roy Hill Member. See also p104, p117, p127, p149, p156, p164.|2629 +/- 5 Ma (upper contact)|Fortescue Group||Intruded by the Karijini Dolerite. Faulted under the MacLeod Member.|Marine shale, tuff, siltstone, pillow basalts and carbonates.|
8896|Jeerinah Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean|Northeast Pilbara Sub-basin; Northwest Pilbara Sub-basin; South Pilbara Sub-basin, Fortescue Basin.|Max age ~2713, Min age 2629+/-5 Ma.|Fortescue Group, sequence 5. Shown with an informal unnamed member.|||Siliciclastic sedimentary rocks, mafic volcanic rocks and minor felsic volcanic rocks; local carbonate rocks, chert, and dolerite sills. Siliciclastic sedimentary rocks, local volcanic rocks, and dolerite sills.|
8896|Jeerinah Formation|72489|6|Mentioned|p12|Archean|Archean|||||||
8896|Jeerinah Formation|72493|5|Briefly described|p30|||Hamersley Basin.||Fortescue Group.|Roy Hill Shale Member.|||
8896|Jeerinah Formation|72569|6|Mentioned|p2|||Of the Hamersley Basin.|||Includes the Nallanaring Volcanic Member.|||
8896|Jeerinah Formation|72712|5|Briefly described|p3,p7, p8, p9, p10 Fig.6. p10, p35.|Neoarchean|Neoarchean|The uppermost unit of the Fortescue Group.Estimated depositional thickness of unit is 400m in Hardey Syncline, but dolerite and gabbro sill intrusions inflate the thickness to 1.8km in places.|c. 2715 Ma to c. 2629 Ma.|Top of the Fortescue Group.||Conformably overlies Bunjinah Formation, Maddina Formation and conformably underlies Marra Mamba Iron Formation, Hamersley Group. Intruded by dolerite sills.|Massive to pillowed basalt, basaltic breccia, sandstone, siltstone, mudstone and chert. More mafic extrusives in S, more sedimentary rocks in N.|
8896|Jeerinah Formation|72758|5|Briefly described|p16 Tb.1, p19, p22, p28, p58.|||This formation is intruded by numerous dolerite sills that may comprise up to 60% of the formation's 940m maximum thickness. Marine environment interpreted. Grat lateral extent suggests more affinity with Hamersley Group than Fortescue Gorup.||Fortescue Group||Conformably overlies Mount Jope Volcanics. Intruded by numerous dolerite sills. Generally transitions upwards into Marra Mamba Iron Formation, but some contacts show angular unconformity.|Thin-bedded mudstone, chert, banded iron-formation, and basalt.|
8896|Jeerinah Formation|73022|6|Mentioned|p2 Fig.1, p3 Fig.2|||||Fortesque Group||Underlies the Marra Mamba Iron Formation, Nammuldi Member.|Organic-rich shale with lesser Fe-chert and minor shale.|
8896|Jeerinah Formation|73290|5|Briefly described|p783-784|||||Topmost Fortescue Group.||Is overlain by Marra Mamba Iron Formation.|Shales.|
8896|Jeerinah Formation|73538|6|Mentioned|p4-5, p7|Neoarchean|Neoarchean|Ages of 2684 +/- 6 Ma and 2690 +/- 16 Ma were reported by Mole et al. (2018). [Written as Jeerinah formation on p4].|2684 +/- 6 Ma, 2690 +/- 16 Ma|Fortescue Group||Underlain by Maddina Formation / Bunjinah Formation. Overlain by Nammudi Member, Marra Mamba Iron Formation, Hamersley Group.|Mudstone/siltstone.|
8951|Jigalong Formation|41768|2|Defined|Table 5|Precambrian||See also P41||||||
8951|Jigalong Formation|44142|5|Briefly described|p315 Tb.4-4, p323|||A distinctive marker horizon. >50m thick lenticular unit of proximal submarine fan and turbidite deposits.||Manganese Subgroup||Overlies Enacheddong Dolomite or Stag Arrow Formation conformably. Overlain disconformably by Balfour Formation.|Basal matrix-supported conglomerate, sandstone, shale; capped by a distinctive green silicified mudstone (chert), locally brecciated and glauconitic.|13-MAR-18
8951|Jigalong Formation|60535|5|Briefly described|p556 Fig.1|Mesoproterozoic|Mesoproterozoic|Of the Manganese Group (Bangemall Supergroup).||||||
8951|Jigalong Formation|66107|5|Briefly described|p4 Fig.1 |Mesoproterozoic|Mesoproterozoic|||Of the Manganese Group||Overlies Enachedong Dolomite. Is overlain by Balfour Formation.||
8951|Jigalong Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||chert, sandstone, conglomerate, greensands|
8955|Jilyili Formation|22589|6|Mentioned|p125||Proterozoic|||||||
8955|Jilyili Formation|22816|5|Briefly described|p8 Table 1|||Savory Group||||||
8955|Jilyili Formation|22901|6|Mentioned|76 fig 2|||||||||
8955|Jilyili Formation|22907|5|Briefly described|42|||Geol province Officer Basin. Parent Sunbeam Group.||||||26-MAY-09
8955|Jilyili Formation|23156|4|Described|p15|Neoproterozoic|Neoproterozoic|For location of type area see p15.  The Jilyili Formation is host to at least four large coarse-grained dolerite intrusions see p18 for details.||||||28-SEP-12
8955|Jilyili Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
8955|Jilyili Formation|24535|5|Briefly described|p4 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of Salvation Group. See also misspelt Jiliyili Formation p2.||||||
8955|Jilyili Formation|42708|5|Briefly described|Plate 1|Proterozoic||Reserved as Jilyili.||||||
8955|Jilyili Formation|43209|5|Briefly described|map legend||Neoproterozoic|Of Savory Group.||||||
8955|Jilyili Formation|43229|5|Briefly described|Map Legend||Neoproterozoic|Of Savory Group.||||||26-MAY-09
8955|Jilyili Formation|43492|4|Described|9|||||||||
8955|Jilyili Formation|43756|6|Mentioned|Fig.1,p535|||||||||
8955|Jilyili Formation|62453|6|Mentioned|p52, 16|||Of the Salvation Group.||||||
8955|Jilyili Formation|64580|4|Described|map legend||Mesoproterozoic|Of Salvation Group. Sandstone and siltstone; minor shale, mudstone, and conglomerate.||||||09-DEC-08
8955|Jilyili Formation|64772|5|Briefly described|p13, Plate 1  legend|Mesoproterozoic|Mesoproterozoic|Of the Salvation Group. Sandstone and siltstone; minor shale, mudstone and conglomerate.||||||01-MAR-11
8955|Jilyili Formation|64793|6|Mentioned|p283 fig 2|Cryogenian|Cryogenian|Of NW Officer Basin.||||||
8955|Jilyili Formation|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Savory Basin. Arenaceous. Part of Supersequence 1.||||||
8955|Jilyili Formation|65416|5|Briefly described|p140, p145.|Neoproterozoic|Neoproterozoic|Savory Sub-basin. Correlated with Lefroy Formation. Deposited by NW-directed currents in a marine-modified delta.||||Overlies Glass Spring Formation. Is overlain unconformably by Spearhole Formation.|Interbedded sandstone, siltstone and shale with minor mudstone and conglomerate.|
8955|Jilyili Formation|69091|5|Briefly described|p202|Mesoproterozoic|Mesoproterozoic|Salvation Basin. Age: late Mesoproterozoic.|||||Siliciclastic sedimentary rocks.|
8955|Jilyili Formation|69185|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Unit of Salvation Group.||||
8955|Jilyili Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||shale, mudstone, conglomerate, sandstone|
8955|Jilyili Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Salvation Basin. ||Salvation Group|||Sandstone and siltstone; minor shale, mudstone, and conglomerate.|
8964|Jimperding Gneiss Complex|24160|5|Briefly described|p107-108, p113 Fig.49.|Archean|Archean|South-West Terrane, Yilgarn Craton.|||||Quartzite, gneiss, schist, BIF, ultramafic rocks, banded quartzo-feldspathic orthogneiss; minor calc-silicate.|
8964|Jimperding Gneiss Complex|24410|5|Briefly described|p105, p156|||Granitic rocks partly recrystallised in greenschist facies. Even-grained, seriate, or porphyritic granites, metasedimentary rocks, unltramafic rocks, banded quartzo-feldspathic orthogneiss. Geological Province: Yilgarn Craton.||||||24-NOV-09
8964|Jimperding Gneiss Complex|42533|6|Mentioned|p95|||Variation on Jimperding Orthogneiss?||||||
8964|Jimperding Gneiss Complex|42928|5|Briefly described|p450|||||||||
8964|Jimperding Gneiss Complex|43061|5|Briefly described|p11|||||||||
8964|Jimperding Gneiss Complex|44149|5|Briefly described|p14-15, p27-30, p32, p46|Mesoarchean|Paleoarchean|Metasedimentary rocks and granite, all strongly deformed. Crystallisation age (Nieuwland and Compston, 1981). Detrital zircon age of 3341 +133/-73 Ma; metamorphic ages of c.3180 Ma.|3267 +48/-25 Ma (Zircon U-Pb).|Porlell Subgroup|||Fuchsite-bearing quartzite, quartz-feldspar-biotite-garnet (-orthopyroxene) gneiss, andalusite and sillimanite schist, BIF, minor calc-silicate gneiss, mafic and ultramafic rocks, banded quartzo-feldspathic orthogneiss; granite intrusions.|
9024|Joolabroo Conglomerate|23815|4|Described|p305|||Geological Province: Carnarvon Basin. Max. thickness: 28.5 m.||||||14-DEC-04
9024|Joolabroo Conglomerate|36890|6|Mentioned|p305|||||||||
9033|Jorgenson Monzogranite|22841|5|Briefly described|Map legend||Archean|||||||07-NOV-08
9033|Jorgenson Monzogranite|22890|6|Mentioned|P13|||||||||
9033|Jorgenson Monzogranite|42382|4|Described|p38|||||||||
9033|Jorgenson Monzogranite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
9033|Jorgenson Monzogranite|42742|5|Briefly described|map legend|Archean||||||||07-NOV-08
9033|Jorgenson Monzogranite|42870|6|Mentioned|p80|||||||||
9033|Jorgenson Monzogranite|43074|5|Briefly described|p17,p30.|||||||||
9033|Jorgenson Monzogranite|50075|5|Briefly described|p17|Archean|Archean|Geological Province: Yilgarn Craton.||||||23-DEC-09
9033|Jorgenson Monzogranite|50076|5|Briefly described|Map|Archean|Archean|Biotite monzogranite.  Geological Province: Yilgarn Craton.||||||23-DEC-09
9033|Jorgenson Monzogranite|60076|6|Mentioned|p45 App. 1|||[Agmjo]  Equigranular monzogranite.||||||
9033|Jorgenson Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Equigranular monzogranite; strongly sheared marginal zones.||||||07-FEB-11
9033|Jorgenson Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Equigranular monzogranite; strongly sheared marginal areas.|06-AUG-15
9033|Jorgenson Monzogranite|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean||||||Equigranular monzogranite; strongly sheared marginal areas.|
9033|Jorgenson Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
9033|Jorgenson Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|2726-2600 Ma (inferred)||||Equigranular monzogranite; metamorphosed|
9036|Jowlaenga Formation|7433|6|Mentioned|p44.|||||Unit in Broome Sandstone.||||
9036|Jowlaenga Formation|22776|4|Described|p11, Table.3|Early Cretaceous|Late Jurassic|||||||
9036|Jowlaenga Formation|23722|4|Described|p36|Cretaceous|Late Jurassic|||||||
9036|Jowlaenga Formation|23766|5|Briefly described|p29|Early Cretaceous|Late Jurassic|Parent: Broome Sandstone (but this is also a formation??)||||||26-NOV-08
9036|Jowlaenga Formation|30549|6|Mentioned|p26|||||||||
9036|Jowlaenga Formation|30897|5|Briefly described|p19|||||||||
9036|Jowlaenga Formation|30898|6|Mentioned|Map legend|Cretaceous|Jurassic|Cretaceous or Jurassic||||||
9036|Jowlaenga Formation|32648|6|Mentioned|p32|||U. Jur.||||||
9036|Jowlaenga Formation|33166|6|Mentioned|p67|||Stratigraphy||||||
9036|Jowlaenga Formation|34134|6|Mentioned|Cor.Chart|||Upper Jurassic||||||
9036|Jowlaenga Formation|34363|6|Mentioned|p56|||Jurassic - Cretaceous. See also Fig.7.||||||
9036|Jowlaenga Formation|34495|6|Mentioned|p227|||Upper Jurassic. See PP230, 231,232||||||
9036|Jowlaenga Formation|36224|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Sandstone, fine to medium, well sorted; mudstone interbeds, cross-bedded, bioturbaated; minor conglomerate; fossiliferous.Late Jurassic to Early Cretaceous.||||||01-FEB-05
9036|Jowlaenga Formation|36890|6|Mentioned|p349|||Formerly Jowlaenga Sandstone||||||
9036|Jowlaenga Formation|38589|6|Mentioned|p48|||||||||
9036|Jowlaenga Formation|42814|4|Described|p24|||||||||
9036|Jowlaenga Formation|42815|5|Briefly described|map|Early Cretaceous|Late Jurassic|||||||
9036|Jowlaenga Formation|43281|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
9036|Jowlaenga Formation|44376|14|Not recorded|p4||Neocomian|||||||
9036|Jowlaenga Formation|44997|14|Not recorded|p.14,21,23,34,36-50||Neocomian|On many pages. Neocom.||||||
9036|Jowlaenga Formation|44998|2|Defined|p151-3||Neocomian|Overlain by Melligo Quartzite; Neocomian or uppermost Jurassic. On many pages. p164,183,185-8,196,map.||||||
9036|Jowlaenga Formation|45011|14|Not recorded|p53,64,70-72||Neocomian|(Early Neocomian)||||||
9036|Jowlaenga Formation|45153|2|Defined|App.6-105|Tithonian|Tithonian|Previously Jowlaenga Sandstone||||||
9036|Jowlaenga Formation|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fine to medium grained poorly sorted and commonly ferruginous, fossiliferous, silty sandstone, mudstone, conglomerate|
9036|Jowlaenga Formation|72499|6|Mentioned|p10.|Jurassic|Jurassic|Ref Forman and Wales, 1981. Canning Basin. Part of sequence K along with Jarlemai Fm, Alexander Fm and Wallal Sandstone.|||||Marine sandstone.|
9039|Juan Complex|41094|6|Mentioned|p274|||||||||
9041|Jubilee Member|40617|6|Mentioned|p14|||||||||
9041|Jubilee Member|41271|6|Mentioned|p166|||||||||
9041|Jubilee Member|61155|5|Briefly described|p15|Early Eocene|Early Eocene|Of the Cardabia Calcarenite. Age: ~54Ma. Max. thickness: 110m. Geological Province: Carnarvon Basin/onshore.||||||
9050|Juderina Formation|7161|6|Mentioned|p92, p92 Fig.4, p100, 101|||Neds Creek Basin. Less than 200m thick (from p92 Fig.4).|||||Lagoonal mudrock and barrier-bar sandstone.|
9050|Juderina Formation|7471|5|Briefly described|p8, Map legend|Proterozoic|Proterozoic|Yerrida Basin.||Basal unit in Windplain Subgroup.|Includes Bubble Well Member.|Is overlain by Johnson Cairn Formation.|Quartz sandstone, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|12099|4|Described|p675-9, 680-1, 683, 685-6, Figs.2,4,5,6|Paleoproterozoic|Orosirian|Placed in Glengarry Group by Gee (1987) and Gee and Grey (1993). Unconformably overlies Archean basement.  Pb-Pb model age on Pb-carbonate mineralisation in upper Juderina Formation.|~1650 Ma.|Unit in Windplain Subgroup.|Includes Finlayson and Bubble Well Members.|Intruded by tholeiitic sills of the Killara Formation.|Mature quartz arenites and stromatolitic carbonates.|04-MAR-13
9050|Juderina Formation|22493|6|Mentioned|p92|||||||||
9050|Juderina Formation|22501|6|Mentioned|p117 Fig. 3|||in the Yerrida Province||||||
9050|Juderina Formation|22694|5|Briefly described|p7|||||||||
9050|Juderina Formation|22940|4|Described|Fig.1 p3, p10, Tb2 p12|||Pb-Pb isochron 2258+/-180 Ma (Russel et al., 1994). See also Table 2 p12. of Windplain Subgroup, Yerrida Group.||||||
9050|Juderina Formation|23133|5|Briefly described|p293|||||||||
9050|Juderina Formation|23413|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Windplain Subgroup, Yerrida Basin||||||
9050|Juderina Formation|23561|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup,Yerrida Basin||||||07-NOV-08
9050|Juderina Formation|23581|5|Briefly described|Map legend||Paleoproterozoic|Of the Windplain Subgroup in the Yerrida Group in the Yerrida Basin||||||07-NOV-08
9050|Juderina Formation|23586|4|Described|p15|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23589|3|Fully described|p15|Rhyacian|Rhyacian|2173+/-11[+/- should be 64] Ma (Pb-Pb isochron from Bubble Well Member). Of Windplain Subgroup. Overlying unit Johnson Cairn Formation. Max. thickness: 500 m.||||||13-NOV-13
9050|Juderina Formation|23593|4|Described|P7|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup. Overlying unit Johnson Cairn Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23597|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: 2258+/-180 Ma (Pb-Pb isochron). Of Windplain Subgroup. Overlying unit Johnson Cairn Formation. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23600|4|Described|p8|Proterozoic|Proterozoic|Of Windplain Subgroup. Overlying unit Johnson Cairn Formation. Geological Province: Yerrida Basin. Max. thickness: 1000 m.||||||
9050|Juderina Formation|23611|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|See also page 33 Appendix 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23744|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin. Max. thickness: ~700 m.  See also p10 table 1.||||||07-NOV-08
9050|Juderina Formation|23747|5|Briefly described|p2 Fig 1|Paleoproterozoic|Paleoproterozoic|See also page 4 table 1. Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23748|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Yerrida Group. Geological Province: Yerrida Basin.||||||
9050|Juderina Formation|23749|4|Described|p6|Proterozoic|Proterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||
9050|Juderina Formation|23750|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Windplain Subgroup. Geological Province: Yerrida Basin.||||||
9050|Juderina Formation|23759|4|Described|p15|Paleoproterozoic|Paleoproterozoic|See page 5 Fig 3. Previously "Finlayson Sandstone". Of Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23865|5|Briefly described|p171|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgoup. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|23890|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group. Age: 2173+/-64Ma  Geological Province: Yerrida Basin. See also p21 Fig.11.||||||01-JUL-13
9050|Juderina Formation|24021|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Parent: Windplain Subgroup. Geological Province: Yerrida Basin||||||18-AUG-10
9050|Juderina Formation|24022|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup, Yerrida Group. Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|24028|5|Briefly described|p289|Paleoproterozoic|Paleoproterozoic|Of Windplain Subgroup.  Geological Province: Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|24535|5|Briefly described|p22,23|Paleoproterozoic|Paleoproterozoic|Of the Windplain Group. Geological Province: Yerrida Basin.||||||26-NOV-13
9050|Juderina Formation|40297|6|Mentioned|Fig.1|||||||||
9050|Juderina Formation|40989|4|Described|p15|||||||||
9050|Juderina Formation|42260|6|Mentioned|p125|||||||||
9050|Juderina Formation|43069|1|Redefined|p29|Mesoproterozoic|Paleoproterozoic|Supersedes Juderina Sandstone.||||||24-JUN-09
9050|Juderina Formation|43238|5|Briefly described|p6|||||||||
9050|Juderina Formation|43831|5|Briefly described|Map Legend||Paleoproterozoic|Yerrida Basin.||||||07-NOV-08
9050|Juderina Formation|43836|5|Briefly described|Map Legend||Proterozoic|of Windplain Subgroup.||||||
9050|Juderina Formation|43837|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Windplain Subgroup (Yerrida Group). Quartz arenite, local siltstone, chert, breccia and pebble beds.||||||14-APR-11
9050|Juderina Formation|43843|5|Briefly described|Map Legend||Proterozoic|||||||
9050|Juderina Formation|44204|5|Briefly described|Map Legend||Proterozoic|||||||
9050|Juderina Formation|44830|5|Briefly described|Map Legend||Proterozoic|||||||
9050|Juderina Formation|49893|4|Described|p8|Proterozoic|Proterozoic|Of the Windplain Subgroup (Yerrida Group). Geological Province: Yerrida Basin. Overlain by the Johnson Cairn Formation. See also p2 Fig.1||||||24-JAN-06
9050|Juderina Formation|49896|5|Briefly described|p2 Tb. 1|||Of Gee (1979a). Supersedes Juderina Sandstone. Now of the Windlpain Subgroup (Yerrida Group). See also p3 Tb. 2.||||||
9050|Juderina Formation|49912|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Windplain Subgroup (Yerrida Group).  Quartz sandstone; local siltstone, chert breccia and conglomerate.  Geological Province: Yerrida Basin.||||||
9050|Juderina Formation|50222|5|Briefly described|p317, p320 Fig. 3, p321|Paleoproterozoic|Paleoproterozoic|Basal unit of Windplain Group. Contains Bubble Well and Finlayson Members.  Disconformably overlain by shales of Johnson Cairn Formation. Max. thickness: ~1000m. Geological Province: Yerrida Basin. See also p332.||||||14-APR-11
9050|Juderina Formation|50226|6|Mentioned|p425|||Of the Windplain Group.||||||
9050|Juderina Formation|61269|6|Mentioned|p87 Fig.2|||||||||
9050|Juderina Formation|61271|6|Mentioned|p105 Fig.1|||Of the Windplain Group.||||||
9050|Juderina Formation|62289|4|Described|plate 1, p3 Fig. 1, p4 Fig. 2, p6-11|Palaeoproterozoic|Palaeoproterozoic|Of Windplain Subgroup, Yerrida Group; contains Finlayson and Bubble Well Members; conformably overlain by Johnson Cairn Formation; unconformable on or faulted against Archaean basement; quartz arenite; minor siltstone, shale, and pebble beds. Importantly, no basal conglomerates.||||||
9050|Juderina Formation|62353|5|Briefly described|map legend|Proterozoic|Proterozoic|Unit not shown on map. Geol. Prov: Yerrida Basin.||Of Windplain Subgroup, Yerrida Group.|Includes Bubble and Finlayson Members.||Undivided siliciclastic and carbonate sedimentary rock.|14-APR-11
9050|Juderina Formation|63866|5|Briefly described|p165-p166|||Yerrida Basin. Hosts epigenetic lead-carbonate and oxide mineralisation.||Windplain Subgroup|Includes the Bubble Well Member and the Finlayson Member.||Thick sequence of siliciclastic, carbonate and evaporitic sedimentary rocks. Coarse-grained and silicified arenite, sandstone and stromatolitic carbonates.|
9050|Juderina Formation|64384|5|Briefly described|p78 Tb. 8|||Lowermost unit in Glengarry Group. Overlain by Johnson Cairn Shale. Geological province: Glengarry Sub-basin. Quartzite, siltstone, chert breccia.||||||07-FEB-11
9050|Juderina Formation|65264|5|Briefly described|p26-27, p44 Appdx. 1|||Of the Windplain Subgroup (Yerrida Group). Contains the Finlayson and Bubble Well Members. Geological province: Yerrida Basin.||||||07-FEB-11
9050|Juderina Formation|65408|4|Described|pp82-83, p85 Tab 2|Paleoproterozoic|Rhyacian|Predominantly shallow-water to evaporitic environment. Depositional age from basal stromatolitic carbonate.|2258+/-180 Ma Pb/Pb isochron (Russell et al. 1994)|Lower unit in Windplain Subgroup.|Includes Finlayson and Bubble Well Members.|Is transitionally overlain by Johnson Cairn Formation.|Shallow-water arenite; rare fetid carbonate units; silicified evaporitic rocks and stromatolitic carbonate.|21-JAN-22
9050|Juderina Formation|65411|5|Briefly described|p90.|Paleoproterozoic|Paleoproterozoic|||Unit in Glengarry Group.|||Quartz arenite.|22-FEB-17
9050|Juderina Formation|65412|6|Mentioned|p101 Fig.4.|||||||||
9050|Juderina Formation|65419|1|Redefined|p4 Fig.1, p7, pp8-16.|Paleoproterozoic|Paleoproterozoic|Contains strata previously referred to as Finlayson Sandstone (Bunting et al. 1977); Juderina Sandstone (Gee, 1979); Basal quartzite (Elias et al. 1982); and Juderina Formation (Gee 1987, 1990), redefined by Gee and Grey (1993) and Pirajno et al. (1996).  Evaporitic units, carbonates and chert breccia, previously assigned to this unit by Gee and Grey (1993), are now included in Bubble Well Member. Units lying to the NW of the Great Northern Highway on the Bryah sheet are now taken from this unit and assigned to Peak Hill Schist. Thickness to 1000 m.||Unit in Windplain Subgroup.|Includes Finlayson and Bubble Well Members. Included Finlayson Sandstone Member.|Is conformably and transitionally overlain by Johnson Cairn Formation.|Ridge-forming units of creamy, well-sorted quartz arenite, sandy siltstone, siltstone and conglomerate, separated by poorly exposed successions of shale, sandy siltstone, chert brecia (silicified carbonate) and discontinuous thin arenite beds.|13-NOV-13
9050|Juderina Formation|65472|5|Briefly described|p2, p3 Fig.2|||Thickness: 1000 m. Yerrida Basin. Age: from Fig.2, after Pirajno et al. 2004.|2.6 Ma detrital zircon U-Pb SHRIMP youngest age|Windplain Group||Unconformably overlain by Earaheedy Group outliers.||
9050|Juderina Formation|65550|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Windplain Group, Yerrida Basin. Includes Finlayson Member. Quartz sandstone; local sandstone, shale, siltstone, chert breccia and conglomerate.||||||
9050|Juderina Formation|65896|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Yerrida Group, Yerrida Basin. Includes Finlayson Member at base. Siltstone and quartz wacke, with interbedded quartz pebble conglomerate layers and lenses; minor quartz sandstone.||||||
9050|Juderina Formation|65913|5|Briefly described|p2 Fig.1, pp5-6. |Paleoproterozoic|Paleoproterozoic|||Unit in Windplain Subgroup.|Includes Finlayson and Bubble Well Members.|Overlies Finlayson Member. Is overlain by Johnson Cairn Formation.|Arenite, conglomerate; minor carbonate.|
9050|Juderina Formation|66427|5|Briefly described|p51 ||||||Includes the Finlayson Member.|Is overlain unconformably by Yelma Formation.||
9050|Juderina Formation|67269|5|Briefly described|p20-21 Fig.19|Orosirian|Orosirian|Yerrida Basin. Contains stromatolites (described as "form 2 Grey 1994") with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).|c.2173 +/- 11 Ma.|Yerrida Group.||||
9050|Juderina Formation|67855|5|Briefly described|p204 tab 3-1|Paleoproterozoic|Paleoproterozoic|Gascoyne Complex, Nabberu Basin. Shown as Juderina (Finlayson Sandstone) Formation. 250m thick sandstone-chert-shale epeiric-sea facies.||Glengarry Group||||
9050|Juderina Formation|68561|4|Described|GEOL_LUT_CSV folder + GEOCHRON files|Paleoproterozoic|Paleoproterozoic|Yerrida Basin, Capricorn Orogen||Windplain Group|Includes Finlayson Member, Bubble Well Member.||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate|
9050|Juderina Formation|69003|4|Described|p10, p12|||Yerrida Basin. c.1000m thick.|c.2170 Ma (Pb-Pb).|Windplain Group.|Bubble Well Member.|Is overlain conformably by Johnson Cairn Formation.|Includes evaporitic rocks and stromatolitic carbonates.|
9050|Juderina Formation|69152|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Earaheedy Basin [??]. Must be older than 1652+/- 23 Ma K/Ar age of Killara Formation sill. See geochron file 142863.1.pdf (2002), and also 168979.1.pdf 207Pb/206Pb date for maximum age for deposition of 1298+/-29 Ma[??]|||Includes Bubble Well Member, Finlayson Member and 1 unnamed subunit.|Intruded by sill of Killara Formation.|Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|24-SEP-15
9050|Juderina Formation|69166|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic|||Windplain Group|Includes Finlayson Member||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|69583|5|Briefly described|Plate 2|Proterozoic|Proterozoic|Yerrida Basin.||Windplain Group.|||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|69596|5|Briefly described|p9-10|||Yerrida Basin. Most detritus was sourced from the Yilgarn Craton.||Basal Windplain Group.|Bubble Well, Finlayson Members.||Siliciclastic and carbonate rocks.|
9050|Juderina Formation|70153|4|Described|100k_geologyp10_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop14_lut.csv. Yerrida Basin. Age derived from meta-arenite sample (168979.1.pdf) and constrains maximum age of protolith deposition. [?? Age range of parent unit given as 2500 - 1600 Ma].|1298 Ma +/-29 Ma (SHRIMP)|Windplain Group|Includes Bubble Well Member, Finlayson Member.|Is intruded by Killara Formation.|Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|70795|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin|2500-1600 Ma||||Quartz sandstone; local sandstone, shale, siltstone, chert breccia and conglomerate.|
9050|Juderina Formation|70796|5|Briefly described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|West Australian Craton, Yerrida Basin, Capricorn Orogen. See also 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv, Glengarry100_2645_stratig.pdf, Tieraco100_2545_stratig.pdf.|ca. 2500 to 1600 Ma (inferred)|Windplain Group|Includes the Finlayson Member and the Bubble Member.||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate|
9050|Juderina Formation|70804|5|Briefly described|p2, p7, p19, plate 1|||Previously of the Glengarry Group.||Windplain Subgroup|Includes the Finlayson and Bubble Well Members.|||
9050|Juderina Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, chert, sedimentary breccia, sandstone|
9050|Juderina Formation|71269|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen, West Australian Craton. Of Yerrida Basin. Events: Capricorn Orogeny (1817-1772 Ma). See 100k_geologyp_lut.csv, 100k_intergeol_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv,glengarry_100k_geologyp_lut.csv, glengarry_500k_interpgeop_lut.csv.|2170-1600 Ma (inferred)|Unit of Windplain Group.|Includes Bubble Well Member, Finlayson Member.||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|71270|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Capricorn Orogen. Of Earaheedy and Yerrida basins. Events: Capricorn Orogeny (1817 - 1772 Ma). Sample GSWA 168979 (silicified arenite) yielded a weighted mean 207Pb/206Pb date of 1298+\-29 Ma, interpreted to be the maximum depositional age of the sandstone protolith.  See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 1m_geologyp12_lut.csv, 100k_geologysub10_lut.csv.|2170-1600 Ma (inferred)|Unit of Windplain Group.|Includes Bubble Well Member, Finlayson Member.|Intruded by a 1623+\-23 Ma dolerite sill.|Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate|
9050|Juderina Formation|71468|5|Briefly described|p26|||Geological province: Capricorn Orogen, Yilgarn Craton. Maximum depositional age of c. 2180 Ma (Nelson 2002).||||Overlain by Mooloogool Group.||
9050|Juderina Formation|71484|4|Described|p122,124-128,130,133-134,137,139|Rhyacian|Rhyacian|Geological province: Of Yerrida Basin. Outcrops in the S, NE and NW parts of the Yerrida Basin. Thickness: 300-400m in the S, at least 750m to the N. Maximum depositional age of siliciclastic sandstone 2169+\-19 Ma and c. 2180 Ma (SHRIMP; Nelson et al., 2002; Sheppard et al., in prep); deposition coeval with Crispin Conglomerate? Includes a package of metamorphosed and deformed carbonate sedimentary rocks outcropping between the northern margin of the Yilgarn Craton and Yarlarweelor Gneiss Complex, previously mapped as the Millidie Creek Formation. Dating of metamorphic monazite from tourmaline bearing psammitic schist from this unit yields 1992+\-8 Ma for low grade metamorphism, providing a minimum depositional age (Sheppard et al., in prep). May have underwent medium-grade metamorphism and deformation during c. 1960 Ma Glenburgh Orogeny.|2200-2115 Ma|Unit of Windplain Group.|Includes Bubble Well and Finlayson members.|Basal unit of Windplain Group. Overlain by Johnson Cairn Formation. Underlain unconformably by Yilgarn Craton basement rocks.|Cross-bedded and parallel laminated quartz sandstone, sandy siltstone, siltstone and conglomerate.|30-AUG-19
9050|Juderina Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Yerrida Basin.||Windplain Group|||Quartz sandstone; local sandstone, shale, siltstone, chert breccia, and conglomerate.|
9050|Juderina Formation|72389|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Yerrida Basin. Gabanintha 1:100k map sheet 2644.||Windplain Group|||Quartz sandstone, local sandstone, shale, siltstone, chert breccia and conglomerate.|28-AUG-20
9054|Jugurra Sandstone|35711|6|Mentioned|Table 4|||||||||
9070|Julie Formation|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Dolomite, limestone, lenses of sandstone and calcareous sandstone.||||||
9070|Julie Formation|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
9070|Julie Formation|22561|4|Described|p15|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22566|5|Briefly described|p82|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22567|6|Mentioned|Fig 1 on p92|||||||||
9070|Julie Formation|22646|6|Mentioned|Fig 1 on p 98|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22649|6|Mentioned|p 150|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22650|6|Mentioned|Fig 2 on p 157|||||||||
9070|Julie Formation|22651|5|Briefly described|p 175|||||||||
9070|Julie Formation|22746|5|Briefly described|p513, p528|||See also Table 1 p524||||||
9070|Julie Formation|22762|6|Mentioned|p374|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22763|6|Mentioned|Table 1 on p386|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22804|6|Mentioned|p429|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22805|5|Briefly described|p464 & p475|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Amadeus Basin||||||
9070|Julie Formation|22824|6|Mentioned|Fig 7 on p536|||||||||
9070|Julie Formation|22826|6|Mentioned|p570|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|22901|6|Mentioned|78|||Geol province Amadeus Basin||||||
9070|Julie Formation|22907|6|Mentioned|42|||Geol province Amadeus Basin||||||
9070|Julie Formation|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Correlate of Wonoka Formation.||||||
9070|Julie Formation|23287|6|Mentioned|Fig.4|||Age: Upper Ediacarian. of Amadeus Basin.||||||
9070|Julie Formation|23314|5|Briefly described|331 Fig.2|||||||||
9070|Julie Formation|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
9070|Julie Formation|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Neoproterozoic III|Geological Province: Amadeus Basin.||||||
9070|Julie Formation|23806|6|Mentioned|p1122|||||||||
9070|Julie Formation|35798|6|Mentioned|p311|||||||||
9070|Julie Formation|35805|6|Mentioned|Fig.3|||||||||
9070|Julie Formation|35863|6|Mentioned|Table 1|||||||||
9070|Julie Formation|36898|6|Mentioned|p199|||||||||
9070|Julie Formation|37462|4|Described|Table 4.IX|||||||||
9070|Julie Formation|37928|6|Mentioned|Fig.4|||||||||
9070|Julie Formation|37929|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|38157|6|Mentioned|Table VI|||||||||
9070|Julie Formation|38243|6|Mentioned|p359|||||||||
9070|Julie Formation|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|39565|6|Mentioned|p32|||||||||
9070|Julie Formation|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pale brown to red-brown sandstone overlain by oolitic dolomite. Geological Province: Amadeus Basin.||||||14-FEB-06
9070|Julie Formation|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
9070|Julie Formation|40105|6|Mentioned|p311|||||||||
9070|Julie Formation|40740|3|Fully described|p88|||Described p12.||||||28-SEP-06
9070|Julie Formation|40810|6|Mentioned|p3|||||||||
9070|Julie Formation|40906|6|Mentioned|Fig.9|||||||||
9070|Julie Formation|41005|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41039|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41115|5|Briefly described|p1389|||||||||
9070|Julie Formation|41190|6|Mentioned|Fig.4|||||||||
9070|Julie Formation|41203|5|Briefly described|p26|||||||||
9070|Julie Formation|41270|6|Mentioned|Table 1|||||||||
9070|Julie Formation|41429|5|Briefly described|p246|||||||||
9070|Julie Formation|41618|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41717|6|Mentioned|Fig.2|||||||||
9070|Julie Formation|41801|6|Mentioned|p219|||||||||
9070|Julie Formation|41852|6|Mentioned|Table 1|||||||||
9070|Julie Formation|42059|6|Mentioned|Fig.2 P131|||||||||
9070|Julie Formation|42082|6|Mentioned|Fig.3 P323|||||||||
9070|Julie Formation|42504|4|Described|p72|||||||||
9070|Julie Formation|42643|6|Mentioned|Fig.4 P19|||||||||
9070|Julie Formation|42845|6|Mentioned|Fig.2 P497|||||||||
9070|Julie Formation|42886|4|Described|p223|||see also Fig.2 p219.||||||28-SEP-06
9070|Julie Formation|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Dolostone, limestone (both quartzose), sandstone, shale.  Geological province: Amadeus Basin.||||||23-JAN-08
9070|Julie Formation|43105|5|Briefly described|Fig.3,p8|||||||||
9070|Julie Formation|43225|5|Briefly described|Map Legend||Neoproterozoic|||||||
9070|Julie Formation|43503|6|Mentioned|11-50|||from Ediacaran to||||||
9070|Julie Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
9070|Julie Formation|43756|6|Mentioned|p542|||||||||
9070|Julie Formation|44111|6|Mentioned|p.58, Fig. 2|||in Amadeus Basin, presented as "Julie" only in Fig. 2.||||||
9070|Julie Formation|45155|6|Mentioned|Fig.7|||Amadeus Basin||||||
9070|Julie Formation|46730|5|Briefly described|p7|||Overain by Pertaoorrta Group; underlain by Cyclops Member. Geological Province: Amadeus Basin||||||28-SEP-06
9070|Julie Formation|46865|6|Mentioned|Fig.2|||Upgraded P51.||||||
9070|Julie Formation|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
9070|Julie Formation|47035|6|Mentioned|Fig.1|||||||||
9070|Julie Formation|48990|6|Mentioned|p11|||||||||
9070|Julie Formation|49796|6|Mentioned|Sect C BDF 28|||||||||
9070|Julie Formation|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Dolostone, limestone, sandstone - oolitic and stromatolitic.||||||07-FEB-11
9070|Julie Formation|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Pale brown to red-brown sandstone overlain by oolitic limestone.||||||
9070|Julie Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
9070|Julie Formation|61732|3|Fully described|p4 Fig. 3, p98|Marinoan|Marinoan|Conformably overlain by Arumbera Sandstone; overlies Pertatataka Formation. Max. thickness: 600m. Geological Province: Amadeus Basin. See also p5 Tb. 1, p26, p91.||||||07-FEB-11
9070|Julie Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
9070|Julie Formation|62379|5|Briefly described|p7 Fig. 2, p25|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Dolostone, limestone, siltstone, sandstone.||||||
9070|Julie Formation|62453|5|Briefly described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Amadeus Basin.||||||
9070|Julie Formation|62595|5|Briefly described|p29 Fig.6.|Proterozoic|Proterozoic|Ross River area.|||||Dolostone, limestone, sandstone, oolitic and stromatolitic.|
9070|Julie Formation|62903|6|Mentioned|p730 Fig.1|||Amadeus Basin. Presented in figure as Julie.||||overlies Pertatataka Formation; is overlain by Arumbera Sandstone||
9070|Julie Formation|63458|6|Mentioned|p873, p897 Fig.19, |Ediacaran|Ediacaran|Amadeus Basin.||||Overlies Pertatataka Formation. Correlated with Boonall Dolomite. Is overlain by Arumbera Sandstone.||
9070|Julie Formation|63562|6|Mentioned|p338 fig 3,p343, p346 fig 8,p352 fig 10|Ediacaran|Ediacaran|Of Amadeus Basin.||||Is overlain by Arumbera Sandstone.|Shallow-water platform carbonates.|
9070|Julie Formation|64068|6|Mentioned|p51, 224|||Amadeus Basin. Correlated with Elkera Formation, Central Mount Stuart Formation, southern Georgina Basin.||||||
9070|Julie Formation|64625|5|Briefly described|p244-245, p247, p250-251|Neoproterozoic|Neoproterozoic|Amadeus Basin||||Overlies Pertatataka Formation gradationally. Is disconformably overlain by Arumbera Sandstone.|Dolomite with minor sandstone.|
9070|Julie Formation|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Ediacaran|Deposited in the Amadeus Basin during the Centralian 3 event (~600-544 Ma)||||||
9070|Julie Formation|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
9070|Julie Formation|64794|6|Mentioned|p238 fig 2|Ediacaran|Ediacaran|||||||
9070|Julie Formation|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Amadeus Basin. Rank not shown in diagram.||||||
9070|Julie Formation|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p10.|Proterozoic|Proterozoic|See also p15 Fig.15.||||Overlies Pertatataka Formation. Is overlain conformably (gradationally) by Arumbera Sandstone.|Dolostone, limestone, sandstone.|
9070|Julie Formation|64970|6|Mentioned|p719 Fig. 2|Neproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||27-MAY-09
9070|Julie Formation|65233|5|Briefly described|p3 Fig. 2, p7|Neoproterozoic|Neoproterozoic|Conformable on Pertatataka Formation. Geological province: Amadeus Basin.||||||07-FEB-11
9070|Julie Formation|65272|6|Mentioned|p320 Fig.3||Ediacaran|||||||
9070|Julie Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 21 m.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Pale brown to red-brown sandstone.|
9070|Julie Formation|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Amadeus Basin||||||
9070|Julie Formation|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Amadeus Basin||||||
9070|Julie Formation|65410|6|Mentioned|p74.|Neoproterozoic|Neoproterozoic|Amadeus Basin. Part of Supersequence 3. May be correlated with the Boondawari Formation (Savory Sub-basin).||||||
9070|Julie Formation|65416|6|Mentioned|p146.|||Supersequence LP3. Suggested by Perincek (1996) to pre-date the Petermann Ranges Orogeny.||||||
9070|Julie Formation|67326|5|Briefly described|p2, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin. Up to 150m thick. Oolitic platform carbonates.||||Conformably overlies Pertatataka Formation. Is overlain unconformably by Arumbera Sandstone.|A widespread, fairly thin succession of ooid grainstone, dolostone and limestone.|
9070|Julie Formation|67484|5|Briefly described|p294 Tb.1|Ediacaran|Ediacaran|Amadeus Basin. Contains Tungussia julia (Grey and Corkeron, 1998) fossils. Mis-spelt as Julia on p299.||||Overlies Pertatataka Formation. Is correlated with Egan and Wonoka Formations and Boonall Dolomite.||
9070|Julie Formation|67620|5|Briefly described|p5|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.||
9070|Julie Formation|67856|4|Described|p338 fig 4-30, p337, p345, 346|Neoproterozoic|Neoproterozoic|Carbonate unit.Could possibly correlate with Cluttterbuck Formation.||||Overlies Pertatataka Formation in central Amadeus Basin.||
9070|Julie Formation|68030|6|Mentioned|p239|||Amadeus Basin. Correlated to upepr carbonates in the Wonoka Formation.||||||
9070|Julie Formation|68244|6|Mentioned|p666|Neoproterozoic|Neoproterozoic|Central Australia. ContainsTungussia julia, a stromatolite biostratigraphic marker that correlates Julie Fm to Bonney Sandstone (SA) and Egan Formation.||||||
9070|Julie Formation|68270|5|Briefly described|p683-684|Ediacaran|Ediacaran|Amadeus Basin.||||Overlain by lower Arumbera Sandstone. Underlain by Perttatataka Formation.||
9070|Julie Formation|68277|6|Mentioned|p103|||Central Australia. Mid-Ediacaran age. Correlation based on stromatolites.||||Correlated with Egan Formation.||
9070|Julie Formation|68316|6|Mentioned|p778 Fig.1|||||||||
9070|Julie Formation|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
9070|Julie Formation|68473|6|Mentioned|p531|||Amadeus Basin.||||||
9070|Julie Formation|68733|6|Mentioned|p189 Fig.8|Ediacaran||Amadeus Basin.|580 Ma.|||Equivalent to Egan Formation.||05-DEC-17
9070|Julie Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
9070|Julie Formation|69031|6|Mentioned|p4, p9|||Amadeus Basin. Formerly part of Boord Formation (name discontinued).||||Is overlain by Carnegie Formation.||
9070|Julie Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Dolostone, limestone and siltstone with sandstone lenses.|12-JUL-16
9070|Julie Formation|69438|3|Fully described|p23:2-8, 17-18, 20, 24, 43, 60|Ediacaran|Ediacaran|Priess et al. (1978); formerly the Julie Member (of the Pertatataka Formation) of Wells et al. (1967). Raised to Formation status because of its wide distribution and usefulness as a marker interval. Amadeus Basin. Type section is at Ross River. 10-150m thick. Does not occur W of the Gardiner Range: apparently eroded before deposition of Arumbera Sandstone.||||Conformably overlies Pertatataka Formation. Is overlain conformably to disconformably by Arumbera Sandstone. Correlated with Rodda beds and lower Elkera Formation.|A widespread, relatively thin unit of dolostone, limestone (oolitic in part) and siltstone with sandstone lenses; contains sparse stromatolites.|12-JUL-16
9070|Julie Formation|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
9070|Julie Formation|69606|4|Described|p1, p4 fig 2, p5, p6 fig 3, p14|Ediacaran|Ediacaran|c. <500m thick. Previously the Julie Member of Wells et al, 1967. Potential reservoir and seal rock. Amadeus Basin. Age based on stratigraphic position and stromatolite fossil assemblage. Stromatolite fossil assemblage discussed in detail. Outcrop ranges from poor to moderate where it forms a series of low strike ridges of limestone and dolostone. Contact with the Pertatataka Formation is poorly exposed. See also p15 fig 8, p16, p19.||||Conformably and gradationally overlies the Pertatataka Formation. Overlain (locally unconformably) by the Carnegie Formation and Arumbera Sandstone.|Limestone and dolostone that vary from mictritic to ooid and peloidal packstone and grainstone, interbedded with poorly exposed silstone and sandstone that is stromatolitic and oolitic. Evaporites occur near the top of this formation.|14-SEP-22
9070|Julie Formation|69673|5|Briefly described|p63, p73, p84, p86, p88, p91, p99|||At a maximum 150m thick, can be as little as 10m. Sparse stromatolites in places. Potential reservoir rock.||||Overlain by Arumbera Sandstone|Dolostone, limestone and siltstone with sandstone lenses.|
9070|Julie Formation|69937|4|Described|v Fig.1, vi, p3 Tb.1, p32-34, p55-56|Neoproterozoic|Neoproterozoic|Amadeus Basin. Originally a Member of the Pertatataka Formation; upgraded to Formation status by Preiss et al. (1978) because of its wide distribution and usefulness as a marker bed. Likely zircon provenance discussed.|985 +/- 25 Ma (maximum depositional age).|||Conformably overlies the Pertatataka Formation. Is overlain by the Arumbera Sandstone.|Dominantly carbonate sequence (dolostone and limestone), with lesser lenses and beds of sandstone and occasional siltstone. Also contains thickly-bedded ooid grainstones.|
9070|Julie Formation|70018|5|Briefly described|p235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 3 in the northern Amadeus Basin. Correlable to Inindia Beds in the southern Amadeus Basin.||||Overlain unconformably by Arumbera Sandstone. Underlain by Pertatataka Formation.||
9070|Julie Formation|70416|5|Briefly described|p64, p65 Fig.2, p80|Ediacaran|Ediacaran|Amadeus Basin. Now includes part of the former Boord Formation. See Fig.2 for the history of this unit's stratigraphic relationships. Contains the stromatolite Tungussia julia.||||Overlies Pertatataka Formation. Is overlain by Winnall Group. Correlated with upper part of Inindia beds.||
9070|Julie Formation|70752|5|Briefly described|p126 Fig.1|Proterozoic|Proterozoic||||||Stromatolitic dolostone and limestone with lenses of sandstone and calcareous sandstone.|
9070|Julie Formation|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Carnegie Formation or Arumbera Sandstone or Pertaoorta Group. Underlain by Pertatataka Formation.||
9070|Julie Formation|71001|5|Briefly described|p18 Fig.2, p19-20, 27-28|Ediacaran|Ediacaran|Amadeus Basin. Shallow marine deposits. Carbon isotope correlation graph.|~582-565 Ma.|||Overlies Pertatataka Formation. Is overlain by Arumbera Sandstone.|Shallow-marine dolostone.|
9070|Julie Formation|71080|6|Mentioned|p29 fig 20, p30|Ediacaran|Ediacaran|Amadeus Basin. Supersequence 3.|||||Dominantly carbonate-shale, marl in WA, carbonate in NT.|
9070|Julie Formation|71088|6|Mentioned|p8, p15|Neoproterozoic|Neoproterozoic|Amadeus Basin. Formerly the top carbonate unit of the now disused "Boord Formation". Overlain by the Carnegie Formation at the Boord Ridges (Haines et al., 2012). ||||Overlain by the Carnegie Formation and the Arumbera Sandstone.||
9070|Julie Formation|71279|5|Briefly described|p355 Fig.2, p366|Ediacaran|Ediacaran|Amadeus Basin.|||||Sandstone and dolostone.|
9070|Julie Formation|71344|4|Described|p1092, 1094, 1096 -1100, 1102-3|Ediacaran||Amadeus Basin. Stromatolite stratigraphy and carbon isotope chemostratigraphy gives depositional age constraints. Deposited as shallowing upward sequence in a shallow marine environment.|575-565 Ma.|Of Pertaoorta Package.||Conformable on the Pertatataka Formation.|Interbedded sandy limestones/dolostones and calcareous siltstones.|10-NOV-17
9070|Julie Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|985+/-25 Ma (MDA: U-Pb zircon SHRIMP)||||Gritty calcareous medium-grained sandstone.|
9070|Julie Formation|71800|6|Mentioned|p26 fig 3|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Pertatataka Formation. Overlain by the Carnegie Formation, Angas Hill Formation and the Arumbera Sandstone.||
9070|Julie Formation|71801|6|Mentioned|p230-p232, p234-p235, p237|Ediacaran|Ediacaran|Amadeus Basin.||||Overlies the Pertatataka Formation. Overlain by the Arumbera Formation.|Shallow-marine limestone and dolostone.|
9070|Julie Formation|71810|5|Briefly described|Map legend.|Ediacaran|Ediacaran|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Limestone, dolomite, siltstone, and sandstone; stromatolitic; common diagenetic silicification in carbonates.|
9070|Julie Formation|71841|5|Briefly described|p1-2|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Arumbera Sandstone. Underlain by Pertatataka Formation. Grades into Inindia beds.||
9070|Julie Formation|71842|5|Briefly described|p2-3,9|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).  Generally confined to the NE Amadeus Basin, and along northern margin in WA; disappears from outcrop westward from central northern margin.||||Overlain by Arumbera Sandstone. Underlain by Pertatataka Formation.||
9070|Julie Formation|72375|4|Described|p1-2,31-32|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Originally a member of Pertatataka Formation (Wells et al., 1967), then redefined and upgraded to Formation status due to wide distribution and importance as marker bed (Preiss et al., 1978). Contains thickly bedded ooid grainstone of shallow marine origin, indicating an upward-shallowing cycle following deposition fo the deeper water Pertatataka Formation. SHRIMP U-Pb zircon analysis by Kositin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 985+\-25 Ma, significantly older than the inferred depositional age of underlying pertatataka Formation (c. 575 Ma; Maidment 2005). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS AS13CJE027 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p30 for Hf isotopic results and interpretations). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS RD13CJE003 (calcareous sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p31-32 for Hf isotopic results and interpretations).||||Overlain by Arumbera Sandstone. Underlain conformably by Pertatataka Formation.|Predominantly carbonate rocks such as dolostone and limestone, with lenses and beds of sandstone and occasional siltstone.|04-DEC-19
9070|Julie Formation|72489|5|Briefly described|p3, p4 Fig.3, p5 Fig.4, p4, p6, p11|Ediacaran|Ediacaran|Located in the Amadeus Basin.  See also p7 Fig.6, p8. Correlated with Patsy Hill Member of Bonney Sandstone on basis of stromatolite form. Described as late-Ediacaran.||||Partially overlies Pertatataka Formation. Partially underlies Arumbera Sandstone. Partially underlies Goyder Formation.|Includes oolitic carbonate.|
9070|Julie Formation|72516|6|Mentioned|p90|Ediacaran|Ediacaran|Amadeus Basin.||||Equivalent to the Elkera Formation.||02-JUN-21
9070|Julie Formation|72601|5|Briefly described|p3, p7-8, p11-12, p14, p25|Ediacaran|Ediacaran|Amadeus Basin. Previously part of the Pertatataka Formation prior to redefinition by Preiss et al. (1978).||||Underlain by Pertatataka Formation. Overlain, unconformably in part, by the Carnegie Formation, Mu Formation, Arumbera Sandstone and Winnall beds.||
9070|Julie Formation|73085|4|Described|piii, p1, p3, p5, p7, p11, p13-14, p27|Ediacaran|Ediacaran|Amadeus Basin. [Written as ?Julie Formation on p: 3, 7, 11, 13-14]. Contains diagnostic stromatolite taxa. Lithology is here described from a 6-metre-thick interval in drillhole LA05DD01 tentatively assigned to the unit that was previously assigned to the Arumbera Sandstone. Wavy laminae of the unit in drillhole LA05DD01 interpreted as possible stromatolites. Possible oolites also observed.||||Underlain by Pertatataka Formation [and equivalents]. Overlain by Arumbera Sandstone. Equivalent to Inindia beds.|[Possibly] grey to brown, massive or planar to wavy laminated, recrystallised carbonate rock.|
9070|Julie Formation|73086|2|Defined|p3, p5-6, p99, p122, p132-136, 143|Ediacaran|Ediacaran|[Defined herein. See also definition card, ASUD]. Post-glacial transgressive unit. Amadeus Basin. Part of Supersequence III. Type section: Ross River. Key localities: east of Phillipson Pound. Parts of the unit contain the diagnostic Tungussia julia stromatolite. Previously part of the Pertatataka Formation. A detrital zircon maximum depositional age (youngest grain) of 985 +/- 25 Ma (SHRIMP U-Pb) is significantly older than the inferred true depositional age.||||Conformably underlain by Pertatataka Formation. Overlain by Arumbera Sandstone. Correlates to Rodda beds, Marchinbar Sandstone, Elkera, Central Mount Stuart, Andagera, and Elcho Island formations.|Medium- to coarse-grained and sandy, dark grey dolostone with interbeds of pink, yellow and grey dolostone that are oolitic and sandy, and local dark grey and blue foetid limestone.|
9070|Julie Formation|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||||Underlain by Pertatataka Formation. Overlain by Arumbera Sandstone.||
9070|Julie Formation|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Conformably overlies the Pertatataka Formation, conformably underlies the Carnegie Formation and Arumbera Sandstone.||
9075|Junction Dolerite|22596|6|Mentioned|Table 1 p409|Archean|Archean|||||||07-NOV-08
9075|Junction Dolerite|23137|4|Described|p245 Table.2|||||||||
9075|Junction Dolerite|23853|4|Described|p833, p835|||||||||
9075|Junction Dolerite|23926|6|Mentioned|p16 Fig. 5|||||||||
9075|Junction Dolerite|41368|6|Mentioned|Table 1|||||||||
9075|Junction Dolerite|41890|5|Briefly described|Table 1|||||||||
9075|Junction Dolerite|42117|5|Briefly described|Table 1 P67|||||||||
9075|Junction Dolerite|42221|6|Mentioned|Table 1 P6|||||||||
9075|Junction Dolerite|42344|5|Briefly described|p52|||||||||
9075|Junction Dolerite|42696|6|Mentioned|Plate 1B|Archean||||||||07-NOV-08
9075|Junction Dolerite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
9075|Junction Dolerite|42870|5|Briefly described|Table 1, P67|||||||||
9075|Junction Dolerite|43102|5|Briefly described|Fig.3|||||||||
9075|Junction Dolerite|43162|6|Mentioned|5|||||||||
9075|Junction Dolerite|43496|6|Mentioned|15|||Age: 2762+/-32Ma||||||03-MAR-10
9075|Junction Dolerite|60514|6|Mentioned|p25 Fig. 2, p27 Fig. 4, p31|Archean|Archean|Intrude the Black Flag Group. Age:2680+/-8 Ma. Maximum thickness: 500m. Lateral equivalents of the Golden Mile Dolerite. Geological Province: Yilgarn Craton.||||||07-FEB-11
9075|Junction Dolerite|60623|4|Described|p25 Fig.2|Archean|Archean|Thickness: up to 500m. Intrudes Black Flag Group. Geochemically different from other lavas in area. Lateral equivalents of Golden Mile Dolerite. Divided into 4 internal zones. Geological Province: Eastern Goldfields.||||||07-NOV-08
9075|Junction Dolerite|60627|5|Briefly described|p65 Tb.1|||Intrudes Black Flag Group||||||10-JUN-05
9075|Junction Dolerite|62108|5|Briefly described|p1409 Tb. 14|||Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1417 Fig. 10.||||||07-FEB-11
9075|Junction Dolerite|65834|6|Mentioned|p7, 12, 44|||Kambalda Domain, Kalgoorlie Terrane. Hosts the Junction gold deposit.||Black Flag Group.||||
9075|Junction Dolerite|72057|4|Described|p237-239,246-247,249|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 Condensor 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.|c. 2680 Ma|Unit of Black Flag Group.|||Aphyric basalt, grading upward through dolerite and gabbro into pyroxenite, and up into dolerite, minor gabbro and quartz gabbro.|
9075|Junction Dolerite|72095|5|Briefly described|p10-12,14-17|||Kambalda Region, Eastern Goldfields, Yilgarn Craton. Compositionally indistinguishable from Low-Th Basalt (LTB) of Barnes et al., 2012. Detailed geochemistry is described.||||||
9079|June Hill Volcanics|22484|4|Described|p81 Fig.10|||||||||
9079|June Hill Volcanics|23047|6|Mentioned|36 fig 2|||In the Hamersley Province.||||||10-FEB-09
9079|June Hill Volcanics|23280|5|Briefly described|p1084||Orosirian|Max Age: 1843 (+/-) 2 Ma.||||||
9079|June Hill Volcanics|23325|5|Briefly described|map legend|Precambrian|Precambrian|Of Wyloo Group.||||||
9079|June Hill Volcanics|23575|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Wyloo Group. Overlying unit Ashburton Formation. Underlying unit Duck Creek Dolomite.||||||
9079|June Hill Volcanics|23612|5|Briefly described|p841|Paleoproterozoic|Paleoproterozoic|Age: 1843+/-2 Ma, 1828+/-38 Ma. Of Ashburton Formation.||||||07-NOV-08
9079|June Hill Volcanics|23774|5|Briefly described|p731||Paleoproterozoic|Age: 1843+/-2 Ma (U-Pb) (Pidgeon and Horwitz 1991). Overlying unit: Ashburton Formation - unconformable.||||||07-NOV-08
9079|June Hill Volcanics|23890|5|Briefly described|p5 Fig.2|||Age: 1977+/-165Ma (U-Pb SHRIMP).  Geological Province: Ashburton Basin.||||||
9079|June Hill Volcanics|24544|4|Described|p47 Fig.35|Paleoproterozoic|Paleoproterozoic|Of Upper Wyloo Group. Conformably overlain by Ashburton Formation. Age: 1799+/-8 Ma. Geological Province: Ashburton Province.||||||07-NOV-08
9079|June Hill Volcanics|24602|5|Briefly described|p856-857|||Age: 1799 +/- 8 Ma (SHRIMP) as reinterpreted. Of the Wyloo Group. Overlain by the "Ashburton" siliclastic succession.||||||
9079|June Hill Volcanics|24607|5|Briefly described|p967, p968 Fig. 1, 970|Paleoproterozoic|Paleoproterozoic|Age: 1843 Ma (Thorne & Seymour, 1991) multi-grain U-Pb zircon age in NW Wyloo Dome now believed to be amalgam of crystallisation and inherited zircon. Single grain SHRIMP U-Pb age 1799 +/- 8 Ma is now preferred. Geological Province: Ashburton Basin. Previously considered coeval with Mount Boggola volcanic succession, but the 1829 Ma age for Mt Boggola now seems to make this unlikely.||||Within Ashburton Formation? Or interfingering?||30-NOV-10
9079|June Hill Volcanics|40103|6|Mentioned|Fig.1|||||||||
9079|June Hill Volcanics|40905|6|Mentioned|Fig.1|||||||||
9079|June Hill Volcanics|41845|6|Mentioned|p94|||||||||
9079|June Hill Volcanics|41846|6|Mentioned|p94|||||||||
9079|June Hill Volcanics|42148|6|Mentioned|Table 1 P687|||||||||
9079|June Hill Volcanics|42260|4|Described|p58|||||||||
9079|June Hill Volcanics|42277|5|Briefly described|p61|||||||||
9079|June Hill Volcanics|42435|5|Briefly described|p46|||||||||
9079|June Hill Volcanics|43290|6|Mentioned|p10||Proterozoic|of Wyloo Group? U-Pb zircon date 1840 Ma.||||||
9079|June Hill Volcanics|44477|6|Mentioned|p.12|||SF/50-6.||||||
9079|June Hill Volcanics|50216|5|Briefly described|p208|||Of the Wyloo Group. Geological Province: Ashburton Basin.||||||
9079|June Hill Volcanics|50222|5|Briefly described|p336|Paleoproterozoic|Paleoproterozoic|Geological Province: Ashburton Basin.||||||07-NOV-08
9079|June Hill Volcanics|61526|5|Briefly described|p880, p884|Paleoproterozoic|Paleoproterozoic|Of the Upper Wyloo Group. Age: ca 1840 Ma (U-Pb, Pidgeon and Horwitz 1991). Geological Province: Ashburton Basin.||||||07-NOV-08
9079|June Hill Volcanics|62129|5|Briefly described|p16|Proterozoic|Proterozoic|Age: c. 1840Ma (U-Pb, Pidgeon and Horwitz 1991).||||||07-FEB-11
9079|June Hill Volcanics|63866|4|Described|p152, p154, p177||Statherian|Ashburton Basin. SHRIMP ages are dervied from Evans et al., 2003.|1799 +/- 8 Ma and 1786 +/- 11 Ma (SHRIMP U-Pb)|||Overlain by the Ashburton Formation.|Pumice-breccia sandstone.|
9079|June Hill Volcanics|63869|5|Briefly described|p5, p6|Paleoproterozoic|Paleoproterozoic|Locally developed on WYLOO sheet area. SHRIMP U-Pb zircon from a thick volcaniclastic sandstone and siltstone unit.|1786 +/- 11 and 1799 +/- 8 Ma (Evans et al. 2003)|Unit in Wyloo Group.||||
9079|June Hill Volcanics|64384|6|Mentioned|p46|||Yielded acid tuff or fragmental volcanic rock containing zircons of U-Pb age: 1843+/-2ma. June Hill Volcanics occur locally within upper Wyloo Group.||||||07-FEB-11
9079|June Hill Volcanics|65830|5|Briefly described|p3|Statherian|Statherian|SHRIMP U-Pb zircon ages (Evans et al.,2003). |1799 +/- 8 Ma and 1786 +/- 11 Ma.|Of the Wyloo Group||Overlain by the Ashburton Formation.||
9079|June Hill Volcanics|66115|5|Briefly described|p136, p137 Fig.1, p145-147|Paleoproterozoic|Paleoproterozoic|Age: ca. 1800 Ma (SHRIMP U-Pb, 1806+/-9 Ma Nelson 2002; Sircombe 2003; 1799+/-8 Ma Evans et al. 2003), and a new U-Pb SHRIMP date on tuff reported in this paper: 1795+/-7 Ma zircon typical of magmatic growth and detrital zircon ranging from 1834-3470 Ma.|See comments.|Wyloo Group||Conformably overlies Duck Creek Dolomite (north of Duck Creek Gorge).|Basalt and tuffs.|
9079|June Hill Volcanics|66950|6|Mentioned|p4, p5, p6, p15|Orosirian|Orosirian|||Of the Wyloo Group.||||16-DEC-16
9079|June Hill Volcanics|67056|5|Briefly described|p419 Fig.2, p440. |Paleoproterozoic|Paleoproterozoic|Locally-distributed, bimodal.|c.1800 Ma (Evans et al. 2003).|Unit in Upper Wyloo Group.||Overlies Duck Creek Dolomite. Is overlain by Ashburton Formation.||
9079|June Hill Volcanics|67130|5|Briefly described|p3 fig 2, p5, p25, p24 fig 17|Statherian|Statherian|Up to 120m thick.|1795 +/- 5 Ma|Wyloo Group, Upper||Interbedded with and disconformably overlain by Ashburton Formation. Gradationally overlies Duck Creek Dolomite|Basalt (some pillowed), tuffs, agglomerates and interbedded rhyolite and sandstone.|
9079|June Hill Volcanics|67827|5|Briefly described|p416 Fig.5|Orosirian|Orosirian||~ 1800 Ma|Of the Upper Wyloo Group.||||
9079|June Hill Volcanics|67855|4|Described|p217, p210, p212 fig 3-10, p216 |Paleoproterozoic|Paleoproterozoic|Up to 120m thick at type, but thin northwards.|1977 +/- 165|Of Wyloo Group||Overlies / grades into Duck Creek Dolomite (conformably). Overlain by Ashburton Formation (disconformably).|Mafic lava, tuff and agglomerate interbedded with felsic-volcanic and sedimentary rocks. At base grades into Duck Creek Dolomite followed by 75m of crystal-lithic tuff or coarse pillow-breccia and thin basalt flows.|
9079|June Hill Volcanics|68035|5|Briefly described|p292 fig 6|Statherian|Statherian|Ashburton Basin.|1795+/-5 Ma|Of upper Wyloo Group.||?intrudes Ashburton Formation or under and overlain by Ashburton Formation.|Basalt to rhyolite, sandstone.|
9079|June Hill Volcanics|68280|5|Briefly described|p5, p54|Paleoproterozoic|Paleoproterozoic||1795+/- 5 Ma|||Intrudes Ashburton Formation|Basalt, rhyolite and sandstone.|
9079|June Hill Volcanics|69003|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Ashburton Basin, Capricorn Orogen. Locally-preserved sequence.|c.1799 Ma.|||?Intrudes/occurs within Duck Creek Dolomite.|Sequence of felsic and mafic volcanics.|
9079|June Hill Volcanics|69080|5|Briefly described|p688||||c.1800 Ma (Evans et al., 2003).|Unit in Wyloo Group.||Overlies Duck Creek Dolomite north of the Wyloo Dome.||
9079|June Hill Volcanics|69538|5|Briefly described|p517 Fig.3|Paleoproterozoic|Paleoproterozoic||1800 Ma.|Unit in Wyloo Group.||||
9079|June Hill Volcanics|70327|5|Briefly described|p2-3|||Previous age determinations (1799 +/- 11 Ma, Evans et al. 2003; 1795 +/- 7 Ma, Wilson et al. 2010) are from unconformably overlying strata and do not give the eruptive age of this unit.||||||17-OCT-16
9079|June Hill Volcanics|71112|5|Briefly described|p75|||Geological province: Pilbara Craton. ||||Overlain by Upper Ashburton Formation. Underlain by Lower Ashburton Formation.||
9079|June Hill Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basalt, agglomerate, crystalline dolostone/dolomite andesite|
9079|June Hill Volcanics|71273|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.||Wyloo Group.|||Mafic, intermediate and felsic volcanic rock; minor interbedded sedimentary rocks.|
9079|June Hill Volcanics|71808|6|Mentioned|p119, p149|||Ashburton Basin.|1843 +/- 2 Ma|Wyloo Group, Upper||||
9079|June Hill Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Ashburton Basin.||Wyloo Group|||Mafic, intermediate, and felsic volcanic rock; minor interbedded sedimentary rocks.|
9079|June Hill Volcanics|72570|6|Mentioned|p3 fig 1|Statherian|Statherian||c. 1790 Ma|Wyloo Group||||
9079|June Hill Volcanics|72712|5|Briefly described|p25, p34, p45.|Statherian|Statherian|Not described in report as not found in study area.|1795 +/- 7 Ma.|Wyloo Group||Overlies Duck Creek Dolomite and disconformably overlain by Ashburton Formation.|Includes volcanics.|
9079|June Hill Volcanics|72758|5|Briefly described|p4 Fig.1, p12 Tb1, p31, p33, p35-37.|||Confined to area north of the Wyloo Dome. Up to 120 thick around June Hill. Thin and wedge out northwards over c. 45km. See also p40. Contact with Duck Creek Dolomite is transitional N of June Hill where thin beds of tuff and basalt are interbedded with dolomite..||Wyloo Group||Conformably overlies Duck Creek Dolomite and disconformably underlies Ashburton Formation.|Mafic lavas (some pillowed), tuffs, and agglomerates, interbedded with felsic volcanics and sedimentary rocks (minor dolomite, sandstone and mudstone).|
9079|June Hill Volcanics|73214|5|Briefly described|p985|||Ashburton Basin. Geochronology by Evans et al. (2003).|1799 +/- 8 Ma; 1786 +/- 11 Ma.|||||
9090|Jurabi Member|23726|5|Briefly described|p93 Fig 29|||Overlying unit Milyering Member. Underlying unit Tantabiddi Member||||||
9090|Jurabi Member|33593|2|Defined|p114|Pleistocene|Pleistocene|Prob. Pleistocene||Of Bundera Calcarenite.||||16-APR-18
9090|Jurabi Member|35796|6|Mentioned|p288|||||||||
9090|Jurabi Member|37016|6|Mentioned|Map legend|Holocene|Pleistocene|Pleistocene to Holocene.||||||
9090|Jurabi Member|39427|4|Described|Table 1|||||||||
9090|Jurabi Member|41271|4|Described|p194|||||||||
9090|Jurabi Member|42116|6|Mentioned|Fig.28 P72|||||||||
9090|Jurabi Member|66125|5|Briefly described|p133 Fig.4|||Ningaloo Reef area; onshore. Occupies a terrace between the Tantabiddi and Jurabi Scarps.||Bundera Calcarenite.|||Coarse-grained littoral deposits overlain by medium-grained aeolian deposits.|
9093|Jurgurra Sandstone Member|7433|5|Briefly described|p43. |Jurassic|Jurassic|||Unit in Wallal Sandstone.|||Sandstone, mudstone and conglomerate; partly eolian.|
9093|Jurgurra Sandstone Member|22767|5|Briefly described|Table3 P12, P23|Late Jurassic|Early Jurassic|Of Wallal Sandstone.||||||
9093|Jurgurra Sandstone Member|22776|6|Mentioned|p20|||Parent:Wallal Sandstone.||||||
9093|Jurgurra Sandstone Member|36634|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|Early ? to Late Jurassic.||||||
9165|Kambalda Komatiite|22666|4|Described|p696, Fig.1b|Archean|Archean|Age of unit 2706+/-36 Ma (Foster et al., 1996).||||||07-NOV-08
9165|Kambalda Komatiite|23130|5|Briefly described|p348|||||||||
9165|Kambalda Komatiite|23137|4|Described|p245 Table.2|||Of Kalgoorlie Group.||||||14-APR-08
9165|Kambalda Komatiite|23139|4|Described|p234 Fig.2, p235|||||||||
9165|Kambalda Komatiite|23862|5|Briefly described|p30 Tb. 1, p34|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
9165|Kambalda Komatiite|23926|5|Briefly described|p17|||||||||
9165|Kambalda Komatiite|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
9165|Kambalda Komatiite|24196|5|Briefly described|p47 Fig. 5|||Overlain by the D.C. Basalt. Overlies the Lunnon Basalt . Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||
9165|Kambalda Komatiite|41368|6|Mentioned|p73|||||||||
9165|Kambalda Komatiite|41644|6|Mentioned|p219|||||||||
9165|Kambalda Komatiite|41890|5|Briefly described|p278|||||||||
9165|Kambalda Komatiite|42117|5|Briefly described|p67|||See also Table 1||||||
9165|Kambalda Komatiite|42118|6|Mentioned|p88|||||||||
9165|Kambalda Komatiite|42221|5|Briefly described|p9|||||||||
9165|Kambalda Komatiite|42329|6|Mentioned|Fig.4 P17|||||||||
9165|Kambalda Komatiite|42406|5|Briefly described|Fig.2 P250|||||||||
9165|Kambalda Komatiite|42696|6|Mentioned|Plate 1B|||||||||
9165|Kambalda Komatiite|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
9165|Kambalda Komatiite|42870|5|Briefly described|Table 1, P67|||||||||
9165|Kambalda Komatiite|43052|5|Briefly described|p48|||||||||
9165|Kambalda Komatiite|43102|5|Briefly described|p5|||||||||
9165|Kambalda Komatiite|43162|6|Mentioned|5|||||||||
9165|Kambalda Komatiite|43496|6|Mentioned|6-15|||Age: 2702+/-4Ma||||||03-MAR-10
9165|Kambalda Komatiite|50556|5|Briefly described|p1116 Fig.6||Archean|Underlies Devon Consols Basalt. Eastern Goldfields Province.||||||07-NOV-08
9165|Kambalda Komatiite|60076|5|Briefly described|p12 Tb. 2|||Ultramafic flows and cumulates.  Max. thickness: 1500m.  Geological Province: Kambalda domain (Yilgarn Craton).||||||02-FEB-05
9165|Kambalda Komatiite|60514|4|Described|p27 Fig 4, p28, p41 Fig. 11, p65 Tb. 1|Archean|Archean|Of the Kalgoorlie Group. Age: 2709+/-4 Ma. Maximum thickness: 1200m. Geological Province: Kambalda Domain, Yilgarn Craton.||||||07-FEB-11
9165|Kambalda Komatiite|60555|5|Briefly described|p5, p6 Fig. 3|Archean|Archean|Underlain by Lunnon Basalt, overlain by basalts comprising Paringa Basalt and Devon Consols Basalt. Thickness: 80-2000m.||||||30-NOV-09
9165|Kambalda Komatiite|60578|5|Briefly described|p5|Archean|Archean|Age: c. 2.7Ga||||||07-NOV-08
9165|Kambalda Komatiite|60623|4|Described|p25 Fig.2|Archean|Archean|Age: 2709+/-4 Ma. Thickness: 100 to >1200 m. High Mg ultramafic flows. Of the Kalgoorlie Group. Geological Province: Eastern Goldfields.||||||13-JUN-13
9165|Kambalda Komatiite|60627|5|Briefly described|p65 Tb.1|||Of Kalgoorlie Group.||||||
9165|Kambalda Komatiite|62108|5|Briefly described|p1409 Tb. 12|||Of the Kalgoorlie Group. Geological Province: Yilgarn Craton (Boulder-Lefroy Shear Zone). Also known as Tripod Hill Formation. See also p1417 Fig. 10.||||||07-FEB-11
9165|Kambalda Komatiite|62109|5|Briefly described|p1428|Archean|Archean|Ultramafic lava flows. Age: 2709Ma. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton.||||||07-NOV-08
9165|Kambalda Komatiite|62110|5|Briefly described|p1442 Fig. 1|||Includes Silver Lake and tripod Hill Members. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
9165|Kambalda Komatiite|62111|5|Briefly described|p1458 Fig. 2|||Of Kambalda Gp. Variably serpentinised or talc-carbonate altered metakomatiite, with intercalated siliceous metasedimentary rocks. See also Kambalda Komatiite Formation. Geol Prov: Kambalda Dome.||||||07-FEB-11
9165|Kambalda Komatiite|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|NW Kambalda Domain. Kambalda Sequence.|||||Komatiite and high MgO basalt.|
9165|Kambalda Komatiite|64340|5|Briefly described|p7|||Underlain by Lunnon Basalt, overlain by Paringa Basalt. Thickness: 80 - +2000m.||||||
9165|Kambalda Komatiite|64633|5|Briefly described|p4 Fig.3, p6 Fig.4, p21.|Neoarchean|Neoarchean|Kalgoorlie Terrane.|2707 +/- 4 Ma (Boorara).|Unit in Kambalda Sequence.||||
9165|Kambalda Komatiite|64715|5|Briefly described|p3, p4, p5 Fig. 4|Archaean|Archaean|Formerly Hannan Lake Serpentinite.Hosts world-class nickel dep.at Kambalda/interpreted as same komatiite outcropping at Mount Hunt.Serpentinite outcrops in lower section on western shore of Hannan Lake.Talc-carbonate alteration at Serpentine Bay - etc.||||||16-DEC-08
9165|Kambalda Komatiite|65204|6|Mentioned|pg6 Tbl.1, p9|Archean|Archean|Komatiitic flows and/or massive olivine adcumulate; metamorphosed.||||||
9165|Kambalda Komatiite|65834|6|Mentioned|p1, 7, 44-47|||Kambalda Domain, Kalgoorlie Terrane. Hosts the Red Hill gold deposit.|c.2700 Ma (Claoue-Long et al., 1988).|Kalgoorlie Group.||||
9165|Kambalda Komatiite|66854|5|Briefly described|pp943-945.|||Forms part of the core of the Kambalda Anticline. Five shale units occur at or near the base; ore is associated with lowest three. Article proposes ore-formation by sulfur-halogen-rich volatiles being mobilised by flattening during folding.||||Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt. Is intruded by granitoids.||
9165|Kambalda Komatiite|66880|5|Briefly described|p7. |Archean|Archean||c.2710-2700 Ma (Claoue-Long et al. 1988).|Unit in Kambalda Sequence.||Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt.||
9165|Kambalda Komatiite|67198|4|Described|p5 fig 2, p81, p83-84, p88, p94 Fig.45|Neoarchean|Neoarchean|See also p114, p116 Fig.50, p118, p131-133, p135. Kalgoorlie Terrane. Nickel sulfide mineralisation detailed. Age determinations detailed. Thickness variations of this unit inferred to be controlled by the Transfer and Mont Blanc Faults. See also references to Kambalda Komatiite Formation (p84-90).|2708 +/- 4 Ma (U/Pb Nelson 1997)|Kambalda Sequence|Silver Lake Member, Tripod Hill Member|Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt and Paringa Basalt|Komatiite, komatiitic basalt. Dacitic/rhyolitic volcanic rocks and minor intrusions, also with volcaniclastics/tuff.|11-SEP-17
9165|Kambalda Komatiite|68289|5|Briefly described|p6-p7, p11-p13, p29|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. Up to 700m thick. Outcrop localities are provided.|||Includes the Silver Lake Member and the Tripod Hill Member.|Overlies the Lunnon Basalt. Intruded by the Kambalda Granodiorite.||
9165|Kambalda Komatiite|69583|5|Briefly described|p37, p39|||Southern Kalgoorlie Terrane.|||Silver Lake, Tripod Hill, Members.|||
9165|Kambalda Komatiite|69586|5|Briefly described|p10|||Kalgoorlie region.||||Equivalent to Agnew Komatiite.||
9165|Kambalda Komatiite|69619|5|Briefly described|p115, p118-122, p124 Fig.8, p127|Neoarchean|Neoarchean|Constitutes the eastern (foot) wall of the Hampden-Boulder-Jubilee gold mine. c.200m thick.|2692 +/- 4 Ma (minimum) Swager (1997).|||Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt.|A sequence of komatiite flows (talc-chlorite-carbonate ultramafic rock and schist); and thin, discontinuous sedimentary rocks, including definitive shale marker beds at the top.|
9165|Kambalda Komatiite|69631|5|Briefly described|p7, p9, p11, p16, p25|||Kambalda area, Kalgoorlie Terrane. Formerly the Hanna Lake Serpentinite. Hosts Ni  mineralisation along the basal contact.|||Silver Lake, Tripod Hill, Members.|Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt.|Spinifex-textured ultramafic flows with cumulate (dunite or peridotite) bases; locally serpentinised or talc-carbonate altered.|
9165|Kambalda Komatiite|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. ||Unit of Kambalda Sequence.||Overlain by D. C. Basalt. Underlain by Lunnon Basalt.|Komatiite, komatiitic basalt and felsic volcanics.|
9165|Kambalda Komatiite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2717 +/- 4 Ma (isotopic) - 2692 Ma (inferred).|Hannans Subgroup|Includes Tripod Hill Member, Silver Lake Member||Komatiite; basal pyroxenite; peridotite and picrite; minor sedimentary rock; metamorphosed. Carbonaceous shale and fine grained siltstone to chert; as thin interflow units; metamorphosed. Ultramafic schist; talc-tremolite-carbonate.|
9165|Kambalda Komatiite|70275|6|Mentioned|p472|||Kalgoorlie Terrane, Yilgarn Craton.|c.2705 Ma (Nelson, 1997).|||||
9165|Kambalda Komatiite|70290|5|Briefly described|p296-298|||Kalgoorlie district, Yilgarn Craton.|2708 +/- 7 Ma (U-Pb zircon; Nelson, 1997).|Kalgoorlie Group.|||Ultramafic flows. Greenschist facies metamorphism.|
9165|Kambalda Komatiite|70326|4|Described|p335,360,362-365|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. Widely regarded marker horizon across the Kalgoorlie Terrane. Interflow sediment near base on Kambalda Komatiite U-Pb zircon SHRIMP 2709+\-4 (Connors et al., 2005) and 2702+\-4 Ma (Campbell and Hill, 1988). Produced during ~2705 Ma komatiite eruption event. |~2705 Ma|||Overlain by Devon Consols and Paringa basalts. Underlain by Lunnon Basalt.|Komatiite lava.|
9165|Kambalda Komatiite|70773|5|Briefly described|p18 fig 11, p21, |Neoarchean|Neoarchean|Kambalda Domain, Kalgoorlie Terrane. Previously the Hannan Lake Serpentinite. See also p24 fig 16, p25 fig 18, p26.|c. 2705 Ma|Kambalda Sequence|Includes the Silver Lake Member.|Overlies the Lunnon Basalt. Overlain by the Devon Consols Basalt.|Komatiite, preidotite, dacite and rhyolite.|
9165|Kambalda Komatiite|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.||||||
9165|Kambalda Komatiite|71166|5|Briefly described|p19|||Effective hydraulic seal for gold mineralisation. ||||||
9165|Kambalda Komatiite|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the Lunnon Basalt. Overlain by the DC Basalt.||
9165|Kambalda Komatiite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2717+\-4 Ma; 2692 Ma|Unit of Hannans Subgroup.|Includes Silver Lake Member, Tripod Hill Member.||Komatiite; basal pyroxenite; peridotite and picrite; minor sedimentary rock; metamorphosed; carbonaceous shale and fine-grained laminated siltstone to chert; as thin interflow units; metamorphosed; ultramafic schist.|
9165|Kambalda Komatiite|71308|5|Briefly described|p711 Fig.2, p713, p726|||Kalgoorlie Terrane. Extensive unit.|2710-2700 Ma.|Kambalda Sequence.||Overlies Lunnon Basalt.||
9165|Kambalda Komatiite|71309|6|Mentioned|p740 Fig.3|||||||||
9165|Kambalda Komatiite|72049|6|Mentioned|p259-p260|||Kalgoorlie Terrane.||Kambalda Sequence||||
9165|Kambalda Komatiite|72057|6|Mentioned|p238|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton.||||||
9165|Kambalda Komatiite|72095|4|Described|p4, p6-8,10-17,21|||Eastern Goldfields, Yilgarn Craton. Basement to the Kalgoorlie-Kambalda region. Extensively intruded by mafic and ultramafic sills. Composed of Low-Th basalt (LTB) of Barnes et al., 2012. Detailed geochemistry is described.||Unit of Hannans Subgroup.||Overlies Lunnon Basalt. Overlain by a sequence of flow units of Intermediate-Th Basalt (ITB; Barnes et al., 2012) composition at a stratigraphic position consistent with Devon Consols Basalt.|Ultramafic eruptive and intrusive rocks.|
9165|Kambalda Komatiite|72485|6|Mentioned|p3 Fig.2|||||Kambalda Sequence.||||
9165|Kambalda Komatiite|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
9165|Kambalda Komatiite|73391|5|Briefly described|p19, 194, 244, 279, 285, 442|||See also Appendices. Kambalda Domain, Kalgoorlie Terrane. >1000m thick.|2708 Ma.|||Overlies Lower Basalt. Is overlain by the Devon Consols Basalt, Big Dick Basalt, Mount Pleasant Sill and (unconformably) the Kurrawang Formation.||
9165|Kambalda Komatiite|73596|6|Mentioned|p1162|||Kalgoorlie-Kambalda area, Kalgoorlie Terrane.||Hannans Subgroup.||Overlies Lunnon Basalt. Is overlain by Devon Consols Basalt.||
9250|Kanpa Formation|22716|6|Mentioned|table4,p231|Proterozoic|Proterozoic|||||||
9250|Kanpa Formation|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Central Officer Basin.||||||11-APR-08
9250|Kanpa Formation|22901|5|Briefly described|78|||Overlying unit Lupton Formation.||||||11-APR-08
9250|Kanpa Formation|22907|6|Mentioned|41|||Geol province Officer Basin||||||
9250|Kanpa Formation|23314|5|Briefly described|331 Fig.2|||||||||
9250|Kanpa Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
9250|Kanpa Formation|23571|3|Fully described|p1, 8|Neoproterozoic|Neoproterozoic|Formerly known as the "Kanpa beds". Geological Province: Officer Basin. Underlying Unit: Hussar Formation (conformable). Overlying Unit: Steptoe Formation (conformable). Max. thickness: 516m. Contains stromatolites.||||||04-MAY-05
9250|Kanpa Formation|24161|4|Described|p9 Fig.6, p12|Neoproterozoic|Neoproterozoic|Conformably overlies the Hussar Formation. Conformably overlain by the Steptoe Formation. Geological Province: Officer Basin.||||||
9250|Kanpa Formation|24244|6|Mentioned|p2 fig 1, p3|Neoproterozoic|Neoproterozoic|Stated to be formerly 'Babbagoola Beds' (Grey, K., 2002, written comm.). Officer Basin. Equivalent rocks underlie the Paterson Formation in the Gunbarrel Basin. Includes rocks mapped as Neale Beds in the central part of the NEALE 1:250 000 sheet.||||||
9250|Kanpa Formation|24390|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin.||||||
9250|Kanpa Formation|41751|6|Mentioned|p8|||||||||
9250|Kanpa Formation|43756|6|Mentioned|p541|||||||||
9250|Kanpa Formation|44111|6|Mentioned|p.59|||in Officer Basin. Includes Supersequence 1 palynological taxa.||||||
9250|Kanpa Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
9250|Kanpa Formation|50085|5|Briefly described|p11 Fig. 6|Neoproterozoic|Neoproterozoic|Age: <750Ma.  Geological Province: Officer Basin.||||||
9250|Kanpa Formation|50204|5|Briefly described|p49 Fig.1, p51|Neoproterozoic|Neoproterozoic |Of the Officer Basin. Formerly Babbagoola Beds. Now includes the Neale Beds. Probably equivalent to the Neoproterozoic to ?Cambrian siliciclastic and calcareous sedimentary rocks which unconformably underlie the Paterson Formation.|||||Sedimentary rocks.|
9250|Kanpa Formation|50205|5|Briefly described|p59 Fig.1|Neoproterozoic|Neoproterozoic|Of Officer Basin. ||Unit in Buldya Group.|||Sandstone.|
9250|Kanpa Formation|60118|6|Mentioned|p30|Neoproterozoic|Neoproterozoic|Contains halite beds <10m thick. Geological Province: Officer Basin.||||||
9250|Kanpa Formation|61023|5|Briefly described|p15 Fig. 8|Neoproterozoic|Neoproterozoic|Geological Province: Officer Basin. See also p16 Tb. 3.||||||11-APR-08
9250|Kanpa Formation|61272|5|Briefly described|p120 Fig.1|||Overlies the Hussar Formation. Unconformably overlain by Lupton Formation. See also p123 Fig.4||||||
9250|Kanpa Formation|61716|5|Briefly described|p642|Neoproterozoic|Neoproterozoic|Contains Keene Basalt within drill core Lancer 1.  Age: ca780-720Ma.||||||
9250|Kanpa Formation|61732|5|Briefly described|p4 Fig. 3, p37|Torrensian|Torrensian|Age: 725+/-11Ma (U-Pb SHRIMP, Nelson 2002). Geological Province: central  and southern Officer Basin. See also p58 Fig. 22, p84, p131.||||||07-FEB-11
9250|Kanpa Formation|62453|3|Fully described|p5 Fig. 3, 22, 32|Cryogenian|Cryogenian|Of Buldya Gp. Geol. Prov: Officer Basin. Overlies: Browne Fm. Underlies: Steptoe Fm. Conformably overlies: Hussar Fm. Dolomite, mudstone, shale, siltstone and sandstone, some evaporites and chert. Intercalated with Keene Basalt.||||||
9250|Kanpa Formation|62987|5|Briefly described|p30|||Of the Buldya Group. Geological Province: Officer Basin.||||||
9250|Kanpa Formation|63022|5|Briefly described|p1015, p1016 Fig. 2|Neoproterozoic|Neoproterozoic|Of Buldya Group. Overlies Hussar Formation. Max. age: 779+/-6Ma. Min age: 725+/-11Ma (SHRIMP U-Pb). Geol.Province: Officer Basin. Shallow marine deposits - mixed carbonate-siliciclastic succession of dolostone, siltstone, claystone and sandstone.||||||10-AUG-07
9250|Kanpa Formation|64103|5|Briefly described|p400|Cryogenian|Cryogenian|Of Buldya Group. Age: 725+/-11Ma (age of youngest concordant detrital zircons. Grey et al. 2005). Geological Province: Officer Basin.||||||07-FEB-11
9250|Kanpa Formation|64325|5|Briefly described|p80, p82 Fig. 2|Neoproterozoic|Neoproterozoic|A unit of Supersequence 1. Geological Province: western Officer Basin. Sandstone , dolomite, shale and minor evaporite deposits.||||||
9250|Kanpa Formation|64580|4|Described|map legend||Neoproterozoic|Of Buldya Group. Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.||||||09-DEC-08
9250|Kanpa Formation|64793|5|Briefly described|p283-295|Cryogenian|Cryogenian|Of Officer Basin. At Empress-1A well top 50m is karstified. Age inferred from Fig.3.|c.770 - c.750 Ma.|||Overlies Hussar Formation. Correlated with Skillogalee Dolomite.|Interbedded dolomite (with abundant stromatolites), mudstone and sandstone; intervals of siltstone.|
9250|Kanpa Formation|64796|5|Briefly described|p181, p183 fig 2, p185, p200 Fig.10 |Neoproterozoic|Neoproterozoic|See also p203, p206. Officer Basin.|||||Interbedded dolomite, mudstone, sandstone.|
9250|Kanpa Formation|64797|6|Mentioned|p153 Fig.2|Cryogenian|Cryogenian|Officer Basin. Lithology/rank not shown on diagram.||||||
9250|Kanpa Formation|64970|5|Briefly described|p717, p719 Fig. 2, p 721 Fig. 5, 6, 7.|Riphean|Riphean|Overlie Townsend Quartzite. Geological Province: Officer Basin.||||||27-MAY-09
9250|Kanpa Formation|65102|4|Described|p365,366,367,371 Figs. 4-41,4-43|Neoproterozoic|Neoproterozoic|Officer Basin. 300-600m, shale, pyritic with siltstone; sandstone & dolomite layers; sabkha to shallow marine; conformable on Hussar Formation, conformably overlain by Steptoe Formation; type section in Kanpa 1A, 1301-1817m, contains Neoproterozoic sporomorphs.||||||
9250|Kanpa Formation|65363|3|Fully described|p1, p6 Fig.5, pp8-9. |Neoproterozoic|Neoproterozoic|Officer Basin. Includes elements of Baicalia burra Stromatolite Assemblage, and possibly the megascopic alga Chuaria sp. Correlated with the Tarcunyah Group, and the Burra Group of the Adelaide Rift Complex. Two samples yielded TOC greater than 0.5%. The base of this Formation has a potential regional reservoir seal. Porosity and permeability are discussed. The top of this unit is possibly karstified and almost certainly eroded.|c.780 - 720 Ma.|Unit in Buldya Group.||Overlies Hussar Formation. Is overlain by Wahlgu Formation.|Upper part: seven major dolostone units, grey, pure to sandy, partly stromatolitic, local thin mudstone and sandstone interbeds. Lower: pale, well-sorted and rounded sandstone intervals grading upwards into mudstone or claystone intervals.|
9250|Kanpa Formation|65364|5|Briefly described|p81|||Officer Basin.||||Overlain by Wahlgu Formation, underlain unconformably by Keene Basalt.|Brown to grey claystone and mudstone, grey stromatolitic dolostone, grey to brown sandstone.|16-MAR-12
9250|Kanpa Formation|65365|5|Briefly described|p1, 3-5, 7, 8, 9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Of Buldya Group, western and central Officer Basin. Includes stromatolite assemblage. ||||||
9250|Kanpa Formation|65366|5|Briefly described|p19, 20, 21, 23 Fig. 3, p24|Cryogenian|Cryogenian|Of the Buldya Group, western Officer Basin. Includes the Baicalia burra Stromatolite Assemblage||||||
9250|Kanpa Formation|65368|5|Briefly described|p13, p14 Fig. 1, p16 Fig. 2., p17 Fig. 4|Neoproterozoic|Neoproterozoic|Red mudstones and sandstones.||||||19-MAR-12
9250|Kanpa Formation|65371|5|Briefly described|p53, 54 Fig. 1, p55-57, p58|||Of Buldya Group, Officer Basin. Conformable over Hussar Formation. Disconformably overlain by Wahlgu Formation. Claystone, mudstone, stromatolitic dolostone, sandstone. Shallow marine-coastal. Mineralogy discussed.||||||
9250|Kanpa Formation|65410|6|Mentioned|p72, p76, p78.|||Contains a palynological assemblage of large acritarchs resembling Cerebrosphaera, coenobial aggregates and leiospheres. Thermal alteration of palynological samples indicates maturation to liquid petroleum to dry gas-generation phase.||||||
9250|Kanpa Formation|65416|5|Briefly described|p137, p138 Fig.3, p141.|Late Proterozoic|Late Proterozoic|Officer Basin. Part of Sequence LP1B of Supersequence PL1. Sabkha, some shallow marine, environments. Shales in this unit provide potential seals for the porous sandstones.||||Conformably overlies Hussar Formation. Is overlain conformably by Steptoe Formation.|Interbedded shale, siltstone, claystone and anhydrite with thin sandstone and dolomite layers.|
9250|Kanpa Formation|67195|4|Described|p9 fig 5, p10, p19, p40, 44, 46, 47 |Neoproterozoic|Neoproterozoic|Western Officer Basin. Thermal conductivity of 2.89 W/mK. Basal unit of one well in this study. [Wrongly shown as Cambrian p40]. See also App 1, App 2.||||Overlies Hussar Formation, Mundadjini Formation, overlain by Steptoe Formation.|Sandstone interbedded with siltstone, dolomite with wavy laminations and thick stylolite seams; shale, claystone and mudstone; grey claystone with abundant gypsum crystal. Thick quartz veins occur throughout.|
9250|Kanpa Formation|67200|5|Briefly described|app 2 p7, p9, 10||||||||Finely laminated interbedded siltstone and sandstone with thick quartz veins.|
9250|Kanpa Formation|67269|5|Briefly described|p20-21 Fig.19|Cryogenian|Cryogenian|Officer Basin. Contains Conophyton new form stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).|c.750 Ma.|||||
9250|Kanpa Formation|67454|4|Described|p563, pp564-571.|Neoproterozoic|Neoproterozoic|Officer Basin. Shale beds contain carbonaceous discs tentatively identified as megascopic alga Chuaria sp. Palaeomagnetic results from the Lancer 1 drillhole are detailed and discussed.|c.760 - 720 Ma.|Unit in Buldya Group.|Includes Keene Basalt.|Overlies Hussar Formation conformably.|Lower part mainly mudstone, claystone and sandstone; upper part stromatolitic dolostone, sandstone and mudstone; grey shale beds, possible ash beds, and basalt (Keene Basalt).|
9250|Kanpa Formation|68270|5|Briefly described|p683,687|Cryogenian|Tonian|Western Officer Basin. 725+\-11 Ma maximum depositional age (detrital zircon obtained from upper Kanpa Fm., c. 75 m below the karstified and truncated top of the Buldya Group in Empress 1A), Nelson 2002.||Unit of Buldya Group.||||
9250|Kanpa Formation|68280|6|Mentioned|p26 fig 24|||Officer Basin.||||||
9250|Kanpa Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|Officer Basin.||Buldya Group.||||
9250|Kanpa Formation|69029|6|Mentioned|p328-330|Neoproterozoic|Neoproterozoic|Of Officer Basin. Contains thin organic-rich source rock shales ranging from fair to good oil potental.||||Overlain by Steptoe Formation. Underlain by Hussar Formation.||
9250|Kanpa Formation|69091|5|Briefly described|p30 Fig.3.5, p38 Fig.3.7, see comments|Neoproterozoic|Neoproterozoic|Officer Basin. See also p41 Fig.3.8, p44, p81 Fig.4.17, p108 Fig.5.9, p174 Fig.9.5, p177 Fig.9.6, p182, p200 Fig.10.2.||Buldya Group||Is unconformably overlain by Table Hill Volcanics.|Sedimentary.|26-SEP-14
9250|Kanpa Formation|69152|4|Described|500k_geologyp08_lut||Neoproterozoic|||Buldya Group|||Interbedded medium- and fine-grained sandstone, stromatolitic dolomite, siltstone, and mudstone; in part evaporitic.|06-AUG-15
9250|Kanpa Formation|70153|6|Mentioned|500k_interpgeop14_lut.csv|Cryogenian|Cryogenian|||Buldya Group||||
9250|Kanpa Formation|70793|5|Briefly described|GEOL_LUT_CSV files|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.||Unit of Buldya Group.||||
9250|Kanpa Formation|71001|6|Mentioned|p22, 24|Tonian|Tonian|Officer Basin.|779 +/- 6 Ma (MDA; Piranjo et al., 2006).||Keene Basalt.|||
9250|Kanpa Formation|71268|5|Briefly described|100k_interpgeop_lut.csv|Tonian|Tonian|Of Officer Basin (Phase 1), Centralian Superbasin. Events: Officer Basin Cenozoic diapirism (66-0.01 Ma); Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv.||Unit of Buldya Group.||||
9250|Kanpa Formation|71270|5|Briefly described|500k_interpgeop16_lut.csv|Tonian|Tonian|Of Officer Basin, Centralian Superbasin.||Unit of Buldya Group.||||
9250|Kanpa Formation|72601|6|Mentioned|p6|Cryogenian|Tonian|Geochronologic constraint is a detrital zircon maximum depositional age.|725 +/- 11 Ma SHRIMP U-Pb|||||
9256|Kapai Slate|22534|6|Mentioned|Fig.5 p10|||of Kalgoorlie Group||||||
9256|Kapai Slate|22666|4|Described|p696, Fig.1b|Archean|Archean|Age of unit 2692+/-4 Ma (Claoue-Long et al., 1988).||||||07-NOV-08
9256|Kapai Slate|23057|5|Briefly described|446|||||||||
9256|Kapai Slate|23137|4|Described|p245 Table.2|||Of Kalgoorlie Group.||||||14-APR-08
9256|Kapai Slate|23139|4|Described|p234 Fig.2, p235|||||||||
9256|Kapai Slate|23786|5|Briefly described|p8|Archean|Archean|Of Kambalda Group.  Geological Province: Yilgarn Craton.||||||07-NOV-08
9256|Kapai Slate|23926|6|Mentioned|p10 Tb. 1|||||||||
9256|Kapai Slate|23928|5|Briefly described|p64|Archean|Archean|Geological Province: Yilgarn Craton.||||||07-NOV-08
9256|Kapai Slate|24091|6|Mentioned|p44|||Geological Province: Yilgarn Craton.||||||
9256|Kapai Slate|24139|5|Briefly described|p238|Archean|Archean|Geological Province: Yilgarn Craton.  Age: 2692 +/- 4Ma (zircon).||||||07-NOV-08
9256|Kapai Slate|24169|5|Briefly described|p668|Archean|Archean|Geological Province : Yilgarn Craton.||||||07-NOV-08
9256|Kapai Slate|24196|5|Briefly described|p47 Fig. 5|||Overlain by the Paringa Basalt. Overlies D.C. Basalt. Geological Province: Kalgoorlie Terrane, Yilgarn Craton.||||||
9256|Kapai Slate|24322|5|Briefly described|p61 Fig. 2|Neoarchean|Neoarchean|Age: 2692 +/- 2Ma.  Of the Kambalda Group.||||||07-NOV-08
9256|Kapai Slate|24325|5|Briefly described|p61 Fig. 2|Archean|Archean|Of the Kambalda Group. Overlain by the Paringa Basalt. Overlies the Devon Consols Basalt.  Age: 2692 +/- 2 Ma. Geological Province: Kambalda Dome, Yilgarn Craton.||||||07-NOV-08
9256|Kapai Slate|29681|5|Briefly described|Table 2|||||||||
9256|Kapai Slate|29784|6|Mentioned|Table 1|||||||||
9256|Kapai Slate|30779|6|Mentioned|Table 1|||Stratigraphy||||||
9256|Kapai Slate|30886|5|Briefly described|p19|||Also mention Table 4.||||||
9256|Kapai Slate|30900|6|Mentioned|p67|||On Table 1||||||
9256|Kapai Slate|32685|5|Briefly described|Table 1|||||||||
9256|Kapai Slate|33515|6|Mentioned|p33|||||||||
9256|Kapai Slate|33535|4|Described|p177|||||||||
9256|Kapai Slate|34324|6|Mentioned|p122|||||||||
9256|Kapai Slate|34608|6|Mentioned|p2|||||||||
9256|Kapai Slate|35611|6|Mentioned|Fig.2|||Stratigraphic columns for Kalgoorlie and Kambalda.||||||
9256|Kapai Slate|39895|5|Briefly described|Fig.1|||||||||
9256|Kapai Slate|40005|6|Mentioned|Fig.16|||||||||
9256|Kapai Slate|40083|6|Mentioned|Fig.2|||||||||
9256|Kapai Slate|40849|6|Mentioned|p37|||||||||
9256|Kapai Slate|41066|5|Briefly described|2 of 2 H03|||Mention 1 of 2 L17||||||
9256|Kapai Slate|41249|6|Mentioned|p20|||See also P38||||||
9256|Kapai Slate|41368|6|Mentioned|Fig.1|||||||||
9256|Kapai Slate|41379|6|Mentioned|p42|||||||||
9256|Kapai Slate|41458|6|Mentioned|Fig.5|||||||||
9256|Kapai Slate|41588|4|Described|p245|||||||||
9256|Kapai Slate|41644|6|Mentioned|p219|||||||||
9256|Kapai Slate|41678|6|Mentioned|p27|||||||||
9256|Kapai Slate|41771|5|Briefly described|p25|||||||||
9256|Kapai Slate|41784|6|Mentioned|p65|||||||||
9256|Kapai Slate|41890|5|Briefly described|p278|||||||||
9256|Kapai Slate|42117|5|Briefly described|p67|||See also Table 1||||||
9256|Kapai Slate|42160|6|Mentioned|p45|||||||||
9256|Kapai Slate|42195|6|Mentioned|p146|||||||||
9256|Kapai Slate|42221|5|Briefly described|p10|||||||||
9256|Kapai Slate|42406|5|Briefly described|Fig.2 p250|||||||||07-MAY-21
9256|Kapai Slate|42696|6|Mentioned|Plate 1B|||||||||
9256|Kapai Slate|42735|5|Briefly described|map legend|Archean||||||||07-NOV-08
9256|Kapai Slate|42785|5|Briefly described|Fig.7 P275|||||||||
9256|Kapai Slate|42817|5|Briefly described|p14, Fig.3|||||||||
9256|Kapai Slate|42870|6|Mentioned|Fig.4, P72|||||||||
9256|Kapai Slate|42892|6|Mentioned|Table 3|||||||||
9256|Kapai Slate|43052|5|Briefly described|p48|||||||||
9256|Kapai Slate|43102|6|Mentioned|p4|||||||||
9256|Kapai Slate|43162|6|Mentioned|5|||U-Pb age: 2692+/-4Ma||||||
9256|Kapai Slate|43496|5|Briefly described|6-15|||Age: 2692+/-4Ma||||||03-MAR-10
9256|Kapai Slate|44149|6|Mentioned|p88 Fig.2-90, p91 Tb.2-9|Archean|Archean|Kalgoorlie area, Eastern Goldfields Province.||||||
9256|Kapai Slate|46905|5|Briefly described|Table 1|||Stratigraphic succession||||||
9256|Kapai Slate|50421|5|Briefly described|p285||Archean|2692 Ma. Sedimentary unit intercalated with Upper Basalt. Kalgoorlie Terrane.||||||07-NOV-08
9256|Kapai Slate|50548|5|Briefly described|p1175 Fig.1||Archean|Age: 2692+/-4 Ma.||||||07-FEB-11
9256|Kapai Slate|60076|5|Briefly described|p12 Tb. 2, p21|||Distinct marker beds.  Chert and siliceous slate.  Geological Province: Kambalda domain (Yilgarn Craton).||||||
9256|Kapai Slate|60514|4|Described|p27 Fig. 4, p28 Tb. 1, p29, p36 Fig. 6|Archean|Archean|Overlain by Paringa Basalt, underlain by Devon Consols Basalt. Age: 2692+/-4 Ma. Maximum thickness: 10m. Siliceous sedimentary facies. Geological Province: Yilgarn Craton.||||||07-FEB-11
9256|Kapai Slate|60555|5|Briefly described|p5, p6 Fig. 3|Archean|Archean|Overlain by Paringa Basalt, underlain by Devon Consols basalt.Thickness: >1000m (Swager et al., 1995).||||||30-NOV-09
9256|Kapai Slate|60578|6|Mentioned|p6 Fig.1|Archean|Archean|||||||07-NOV-08
9256|Kapai Slate|60623|4|Described|p25 Fig.2, p29|Archean|Archean|Age: 2692+/-4 Ma. Of Kalgoorlie Group. Conformably overlies Devon Consols Basalt, conformably overlain by Defiance Dolerite. Thickness: less than or equal to 10m. Geological Province: Eastern Goldfields.||||||07-NOV-08
9256|Kapai Slate|62108|5|Briefly described|p1409 Tb. 5|Archean|Archean|Of Kalgoorlie Gp. Varies from pyritic graphitic slate to magnetite-bearing laminated chert; a persistent marker horizon. Age: 2694+/-4Ma. Max. thickn: 25m. Geol Prov: Yilgarn Craton (Boulder-Lefroy Shear Zone). See also p1417 Fig. 10.||||||07-FEB-11
9256|Kapai Slate|62109|5|Briefly described|p1428|Archean|Archean|Sulphidic and tuffaceous shale. Marker horizon between the Devon Consols Basalt and Paringa Basalt above. Age: 2692+/-4Ma. Thickness: 10m. Geological Province: Norseman-Wiluna fold belt/Yilgarn Craton.||||||07-NOV-08
9256|Kapai Slate|62110|5|Briefly described|p1442 Fig. 1|Archean|Archean|Age: 2692+/-4Ma. Geological Province: Kambalda dome in the Norseman-Wiluna greenstone belt, Yilgarn Carton.||||||07-FEB-11
9256|Kapai Slate|62111|5|Briefly described|p1458 Fig. 2|||Of the Kambalda Group. Siliceous metsedimentary unit. Geological Province: Kambalda Dome in the Norseman-Wiluna greenstone belt of the Yilgarn Craton.||||||07-FEB-11
9256|Kapai Slate|62406|6|Mentioned|p54 Fig. 2|||||||||
9256|Kapai Slate|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|NW Kambalda Domain. Kambalda Sequence.|||||Thinly-bedded turbidites and BIF.|
9256|Kapai Slate|64016|6|Mentioned|p56|||Thickness: 0.5 to 10+m. Consists of sulphidic shales and cherts.||||||
9256|Kapai Slate|64340|5|Briefly described|p7|||Underlain by Paringa Basalt, overlain by Devon Consols Basalt.||||||
9256|Kapai Slate|64633|5|Briefly described|p4 Fig.3, p6 Fig.4, p21.|Neoarchean|Neoarchean|Kalgoorlie Terrane.|2692 +/- 4 Ma (Claoue-Long et al. 1988).|Unit in Kambalda Sequence.||||
9256|Kapai Slate|64715|5|Briefly described|p1, p4, p5 Fig. 4|||Overlies Devon Consols Basalt.Cherty sedimentary rock that outcrops as a marker unit. See also p6, p7 Fig. 7.||||||16-DEC-08
9256|Kapai Slate|64771|5|Briefly described|p4|Neoarchaean|Neoarchaean|A clastic sedimentary unit within the upper basalt unit at Kambalda. Maximum deposition age from detrital zircons.|c.2692 Ma (Claoue-Long et al., 1988).|||||
9256|Kapai Slate|65204|6|Mentioned|pg6 Tbl.1|Archean|Archean|Kambalda Domain.||||||
9256|Kapai Slate|65834|6|Mentioned|p7, 44-47, 53-54, 56|||Kambalda Domain, Kalgoorlie Terrane. Co-hosts the Victory and North Orchin gold deposits.||Kalgoorlie Group.|||Sulphidic black shales and cherts.|
9256|Kapai Slate|66880|5|Briefly described|p7, p13. |Archean|Archean|Lies at top of the komatiite at Kambalda. SHRIMP U-Pb zircon date is considered to be the minimum age of komatiitic volcanism. Identical age to Vivien Sequence.|2692 +/- 4 Ma (Claoue-Long et al. 1988).|||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.|Tuffaceous unit.|
9256|Kapai Slate|67020|6|Mentioned|p660.|Archean|Archean||2692 +/- 4 Ma (Claoue-Long et al. 1988)|||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.||
9256|Kapai Slate|67198|4|Described|p5 fig 2, p88|Neoarchean|Neoarchean|See also p118-119, p122, p131-133. Kalgoorlie Terrane. 1-10m thick. A regional marker bed. Age derived from sandstone. Includes zircons as old as 3441 +/- 18 Ma (U/Pb zircon).|2692 +/- 4 Ma (U/Pb detrital zircon)|Kambalda Sequence||Overlies Devon Consols Basalt, is overlain by Paringa Basalt. Is intruded by Kambalda Granodiorite.|Slate, carbonaceous shale,  incised turbidites, minor pale cherty sediments and felsic volcaniclastic rocks.|11-SEP-17
9256|Kapai Slate|68217|4|Described|p71|Precambrian|Precambrian|Approx 10 ft thick [~3m thick]||||Underlain by Devon Consols Basalt. Overlain by Williamstown Dolerite.|Graphitic slate|04-OCT-12
9256|Kapai Slate|68289|5|Briefly described|p6-p7, p11-p13, p29, p31|||Southern Kalgoorlie Terrane. Part of the mafic-ultramafic succession which is overlain by the Black Flag Group. 1-10m thick. Outcrop localities are provided. Contains shallow gold workings which are infilled.||||Overlies the Devon Consols Basalt. Overlain by the Paringa Basalt. Intruded by the Kambalda Granodiorite and Defiance Dolerite.|Slate and chert which at depth becomes carbonaceous and pyriitic.|
9256|Kapai Slate|69035|5|Briefly described|p414 Tb.3, p415 Fig.1, p429|Neoarchean|Neoarchean|~ 1-5 m thick. A persistent marker horizon of black sulphidic mudstone and shale at the top of the Devon Consols Basalt.|2692 +/- 2 Ma, zircon (Claoue-Long et al., 1896)||||Shale.|
9256|Kapai Slate|69583|5|Briefly described|p37, p39|||Southern Kalgoorlie Terrane. 1-10m thick.|c.2692 Ma.|||||
9256|Kapai Slate|69631|5|Briefly described|p7, p11, p14-16, p25, p28|||Kambalda area, Kalgoorlie Terrane. 1-10m thick. Well-exposed as a marker bed.||||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.|Cherty sedimentary rock; at depth, becomes carbonaceous and pyritic slate.|
9256|Kapai Slate|70020|4|Described|p121|Neoarchean|Neoarchean|Geological province: Kalgoorlie Terrane, Yilgarn Craton. ||Unit of Kambalda Sequence.||Overlain by Paringa Basalt. Underlain by D. C. Basalt.|Black shale.|07-MAY-21
9256|Kapai Slate|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Neoarchean||2692 +/- 4 Ma (isotopic age).|Hannans Subgroup|||Black to grey sulfidic slate and silicified shale; subordinate fine-grained volcaniclastic layers and chert, metamorphosed.|
9256|Kapai Slate|70287|6|Mentioned|p188, 190, 195, 210|||Kalgoorlie Gold Field, Eastern Goldfields Province, Yilgarn Craton. Contains 2692 +/- 4 Ma zircons (Claoue-Long et al., 1988).||||Overlies Hannan Lake Serpentinite. Is overlain by Devon Consols and Paringa Basalts.||
9256|Kapai Slate|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Kambalda Domain, Kalgoorlie Terrane, Yilgarn Craton. Age from U-Pb zircon SHRIMP, sampled in Kambalda region (Claoue-Long et al., 1988).|2692+\-4 Ma (Claoue-Long et al., 1988).|||Overlain by Paringa Basalt. Underlain by Devon Consols Basalt. Intruded by Defiance and Williamstown dolerites.||
9256|Kapai Slate|70773|6|Mentioned|p21, p24 fig 16, p25 fig 18|||||||Overlies the Paringa Basalt.|Slate and cherty sedimentary rock.|
9256|Kapai Slate|70863|6|Mentioned|p9|||Kambalda Dome, Yilgarn Craton.||||||
9256|Kapai Slate|71148|6|Mentioned|p122|Neoarchean|Neoarchean|Kalgoorlie Terrane, Eastern Goldfields Superterrane, Yilgarn Craton.||||||
9256|Kapai Slate|71168|5|Briefly described|p9|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton.||||Overlies the DC Basalt. Overlain by the Paringa Basalt.||
9256|Kapai Slate|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Eastern Goldfields Superterrane events (2960 - 2600 Ma); Yilgarn Craton granite magmatism (3010 - 2600 Ma).  See 100k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|2692+\-4 Ma|Unit of Hannans Subgroup.|||Black to grey sulfidic slate and silicified shale; subordinate fine-grained volcaniclastic layers and chert; metamorphosed|
9256|Kapai Slate|71309|6|Mentioned|p740 Fig.3|||||||||
9256|Kapai Slate|72049|5|Briefly described|p253, p255-p256|Neoarchean|Neoarchean|SHIRMP aand LAICPMS analytical techniques and results are discussed in detail. See also p259-p260, p262, p266-p268.|2692 +/- 4 Ma (Claoue-Long et al., 1988)|Kambalda Sequence.||Overlain by the Paringa Basalt.||
9256|Kapai Slate|72095|5|Briefly described|p4, p6-8|Neoarchean|Neoarchean|Eastern Goldfields, Yilgarn Craton. Basement to the Kalgoorlie-Kambalda region. Extensively intruded by mafic and ultramafic sills.|<2692 Ma|Unit of Hannans Subgroup.||Overlies Devon Consols Basalt. Overlain by Paringa Basalt.||
9256|Kapai Slate|72485|6|Mentioned|p3 Fig.2|||||Kambalda Sequence.||||
9256|Kapai Slate|73238|6|Mentioned|p4|||Eastern Goldfields Terrane.||||||
9256|Kapai Slate|73300|6|Mentioned|p1112-1113|Neoarchean|Neoarchean|Yilgarn Craton, Kalgoorlie terrane.|2692 +/- 7 Ma|Kambalda Sequence||Overlies the Devon Consols Basalt, underlies the Paringa Basalt.||
9256|Kapai Slate|73391|5|Briefly described|p24, 194, 238, 244, 304, Appendices.|||Woodall (1965). Kambalda Domain, Kalgoorlie Terrane. Appears as Kapai slate on p194.|2692 +/- 4 Ma (Claoue-Long et al., 1988).|||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.|Graphitic slate; tuffaceous sedimentary rocks. Persistent marker horizon of black sulphidic mudstone and shale.|
9256|Kapai Slate|73596|6|Mentioned|p1162|||Kalgoorlie-Kambalda area, Kalgoorlie Terrane.||Hannans Subgroup.||Overlies Devon Consols Basalt. Is overlain by Paringa Basalt.||
9275|Karara Formation|22589|6|Mentioned|p125||Proterozoic|||||||
9275|Karara Formation|22907|6|Mentioned|41|||||||||
9275|Karara Formation|23364|5|Briefly described|map legend|Proterozoic|Proterozoic|Of Tarcunyah Group, Officer Basin.||||||
9275|Karara Formation|23742|6|Mentioned|p7|||||||||
9275|Karara Formation|23745|6|Mentioned|p15|||||||||
9275|Karara Formation|23760|4|Described|p26|Proterozoic|Proterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
9275|Karara Formation|35387|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9275|Karara Formation|35902|2|Defined|p8|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
9275|Karara Formation|37023|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
9275|Karara Formation|37212|4|Described|p14|||||||||
9275|Karara Formation|38768|6|Mentioned|p81|||||||||
9275|Karara Formation|42278|6|Mentioned|p33|||||||||
9275|Karara Formation|42708|5|Briefly described|Plate 1|Proterozoic||||||||
9275|Karara Formation|43118|5|Briefly described|p16|||||||||
9275|Karara Formation|43229|5|Briefly described|Map Legend||Mesoproterozoic|of Karara Basin||||||
9275|Karara Formation|43348|5|Briefly described|P8, Figure 1 p2||Neoproterozoic|Younger than Yeneena Group||||||
9275|Karara Formation|43697|6|Mentioned|p25|||Sedimentary rocks. Age is Late Proterozoic.||||||08-AUG-05
9275|Karara Formation|43756|6|Mentioned|Fig.1,p534|||||||||
9275|Karara Formation|43849|5|Briefly described|Map Legend||Proterozoic|||||||
9275|Karara Formation|43867|5|Briefly described|p199, Fig.1 p200|||||||||
9275|Karara Formation|44111|6|Mentioned|p.55, 57, p60|||previously thought younger than the Yeneena Group, now included in Tarcunyah Group. Not affected by D4 folding (Miles Orogeny).||||||
9275|Karara Formation|44139|4|Described|p275-276, Fig. 3-67, p278, p282-283|Neoproterozoic|Neoproterozoic|Crowe and Chin (1979). Originally the Karara beds (Williams et al., 1976). Karara Basin, northern Paterson Orogen. Dominantly quartz sandstone; also conglomerate, wacke, feldspathic sandstone, micaceous siltstone, shale, argillite, dolomite and sandy dolomite. Unconformably overlies Yeneena Group, and Rudall Complex. Possibly 5km thick. Age is conjectural; may be >800 Ma.| | ||||05-MAR-18
9275|Karara Formation|44866|5|Briefly described|Map Legend||Neoproterozoic|||||||
9275|Karara Formation|49895|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group. Unconformably overlies the Throssell Group.||||||
9275|Karara Formation|49911|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Tarcunyah Group.  Quartz arenite and quartz-feldspar wacke; minor beds of shale and conglomerate.  Age: c.800Ma.  Geological Province: Officer Basin.||||||
9275|Karara Formation|50008|5|Briefly described|p46 Fig.3||Neoproterozoic|Of Tarcunyah Group. Geological Province: Officer Basin.||||||
9275|Karara Formation|60470|5|Briefly described|p4 Fig. 2|Neoproterozoic|Neoproterozoic|in Officer Basin, of Tarcunyah Group. Lateral equivalent to Gunanya Formation? Sandstone; minor conglomerate, siltstone, and shale||||||
9275|Karara Formation|62453|4|Described|p5 Fig. 3, 64|Cryogenian|Tonian|Geological Province: Paterson Orogen. Of the Tarcunyah Group. Unconformably overlies: Rudall Complex. Conglomerate, sandstone, wacke and shale.||||||
9275|Karara Formation|64580|6|Mentioned|map legend|||Of Tarcunyah Group.||||||15-DEC-08
9275|Karara Formation|64777|5|Briefly described|p3 Fig.4 |Neoproterozoic|Neoproterozoic||||||Sandstone; minor conglomerate, siltstone and shale|
9275|Karara Formation|65102|6|Mentioned|p363, Figure 4-38|Neoproterozoic|Neoproterozoic|Paterson Orogen (NW).||||||
9275|Karara Formation|65403|5|Briefly described|p5, p14, p19. |||Has lithological, stratigraphic and structural similarities with Gunanya Sandstone.||Unit in Tarcunyah Group.||Unconformably overlies Throssell Group.|Mainly quartz arenite; also quartz-feldspar wacke, basal lenses of conglomerate, fining upwards into well-bedded, fine-grained pink sandstone; minor shale beds.|
9275|Karara Formation|65454|4|Described|p9, p11, p30 Fig.A1b|Cryogenian|Cryogenian|Of Tarcunyah Group. Conglomerate that fines upward into well-bedded, fine-grained sandstone. Only part of Tarcunyah Group mapped east of Vines Fault. Unconformably overlies Rudall Complex and Coolbro Sandstone. Upper (sandstone) part was correlated with Gunanya Sandstone (Bagas and Smithies 1998).||||||
9275|Karara Formation|65826|6|Mentioned|p7 Fig.4. |Neoproterozoic|Neoproterozoic|Officer Basin. Shown as lateral equivalent of Gunanya Sandstone.||||||23-MAY-16
9275|Karara Formation|67182|6|Mentioned|p677 Fig.2|Neoproterozoic|Neoproterozoic|||||||
9275|Karara Formation|67202|4|Described|p64-65, p124, p219, p229, p231, p233|Neoproterozoic|Neoproterozoic|See also p235, p243-244, p247, p272. NW Officer Basin. c.350m thick. Speculatively correlated with Choorun and Googhenama Formations. Conductivity image. Hosts a number of Cu, Pb, Zn and Au prospects (locations shown). Has some potential for uranium mineralisation.||Tarcunyah Group.||Unconformably overlies, and is faulted against, Rudall Complex. Correlates with Googhenama Formation.|Coarse-grained arkosic sandstone, pebble conglomerate and thinly bedded dolomite.|
9275|Karara Formation|67430|6|Mentioned|p22|||Paterson Province.||||||
9275|Karara Formation|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|NW Paterson Orogen.||Tarcunyah Group.||||
9275|Karara Formation|69185|5|Briefly described|500k_geologyp08_lut.csv|Neoproterozoic|Neoproterozoic|||Unit of Tarcunyah Group.||||
9275|Karara Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||greywacke, shale, conglomerate, sandstone|
9275|Karara Formation|72034|5|Briefly described|500k_interpgeop16_lut|Cryogenian|Tonian|Gibson Sub-basin, Officer Basin (Phase 1).||Tarcunyah Group|||Fine-grained sandstone, pebble conglomerate, minor siltstone and shale.|
9275|Karara Formation|73168|6|Mentioned|p745-746|Neoproterozoic|Neoproterozoic|Rudall Province. Localised graben development was infilled by the Karara Formation.|ca 800 Ma|||||
9294|Karonie granodiorite|37373|6|Mentioned|Table 2.V|||||||||
9294|Karonie granodiorite|41771|6|Mentioned|Table 1|||||||||
9301|Karrakatta Soil|40367|6|Mentioned|p76|||Of McArthur and Bettanay (1960).||||||07-AUG-07
9303|Karramindie Monzogranite|9168|5|Briefly described|Map legend|Archaean|Archaean||||||Recrystallised biotite monzogranite|
9303|Karramindie Monzogranite|41914|4|Described|p22|||||||||
9303|Karramindie Monzogranite|42698|5|Briefly described|map legend|||||||||
9303|Karramindie Monzogranite|42892|4|Described|p41|||||||||
9303|Karramindie Monzogranite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
9303|Karramindie Monzogranite|60076|5|Briefly described|p45 App. 1|||[Agmka]   Fine- to medium-grained biotite monzogranite; unfoliated.||||||
9303|Karramindie Monzogranite|65204|6|Mentioned|p19 Tbl.4.|Neoarchean||Fine-medium grains; equigranular.||||||
9303|Karramindie Monzogranite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Fine- to medium-grained biotite monzogranite.||||||07-FEB-11
9303|Karramindie Monzogranite|68066|5|Briefly described|p9, p21 Tb. 1, p28, p29, map|Archean|Archean|Forms a few small outcrops in a subcircular area about 7 km2. Ages: (a) Rb-Sr (Turek, 1966); (b) Pb-Pb (Oversby, 1975). Granitoids within greenstone belts - synkinematic.|(a) 2550 +/- 25 Ma; (b) 2705 +/- 30 Ma.||||Recrystallized biotite monzogranite; leucocratic, fine to medium grained, and homogeneous, except for sparse ovoid biotite clots; middle- to upper-amphibolite facies metamorphism, but is not foliated.|
9303|Karramindie Monzogranite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Fine- to medium-grained biotite monzogranite.|06-AUG-15
9303|Karramindie Monzogranite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Fine- to medium-grained biotite monzogranite.|
9303|Karramindie Monzogranite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite|
9303|Karramindie Monzogranite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|2655-2600 Ma (inferred)||||Fine- to medium-grained biotite monzogranite|
9308|Katanga Conglomerate|36883|4|Described|p145|||||||||
9308|Katanga Conglomerate|37460|6|Mentioned|p157|||||||||
9308|Katanga Conglomerate|42260|6|Mentioned|p99|||||||||
9308|Katanga Conglomerate|44477|4|Described|p.12, Table 1||Proterozoic|SF/50-6.||||||
9308|Katanga Conglomerate|44478|14|Not recorded|map legend||Proterozoic|||||||
9315|Kathleen Ignimbrite|30388|4|Described|Table 1|||See also P8. Proterozoic age.||||||
9315|Kathleen Ignimbrite|30390|4|Described|p52|||See also P53-54||||||
9315|Kathleen Ignimbrite|30944|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Pussy Cat Group||||||
9315|Kathleen Ignimbrite|30947|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
9315|Kathleen Ignimbrite|36551|6|Mentioned|Table 31|||||||||
9315|Kathleen Ignimbrite|36886|4|Described|p199|||||||||
9315|Kathleen Ignimbrite|67375|5|Briefly described|p19 Fig.11, p38 Table 1, p47. |Mesoproterozoic|Mesoproterozoic|A mappable unit within the Glyde Formation. Forms a prominent range of hills.|1071 +/- 5 Ma.|Unit in Pussy Cat Group.||Intercalated with and overlain by Glyde Formation.|Flow-banded and lava-like rhyolite, interpreted as a densely-welded and rheomoirphic, originally pyroclastic, deposit. Grades upwards into a eutaxitic, fiamme-textured rock, overlain by lapilli-ash tuffs.|
9315|Kathleen Ignimbrite|67553|5|Briefly described|p20,40-41,48-50,97-104,107-108|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Maximum thickness: 500m. Eruption age at 1071+\-5 Ma (GSWA 195723); coeval with deposition of, and a mappable unit within the Glyde Formation. Thickest in the eastern outcrop area, and thins to the west grading into more homogenous rhyolites, suggesting an eastern volcanic source. Intruded by clastic dykes of Glyde Formation material, indicating rapid deposition of ignimbrite onto semi-consolidated, water-bearing, volcaniclastic sediments.|1071 Ma|Unit of Pussy Cat Group.||Intrudes the Glyde Formation.|Fow-banded and lava-like rhyolite; densely welded and rheomorphic, originally pyroclastic, deposit (rheoignimbrite).|06-AUG-19
9315|Kathleen Ignimbrite|68995|5|Briefly described|p13, p15, p17, p21, p24, p25|||Maximum thickness greater than 500m. Geographically restricted outcrop. See also p27-29, p31 Fig.17, p35 Fig.20, p45-46, p57, p61.||Pussy Cat Group||Overlies the Mount Waugh rhyolite. Overlain by the Glyde Formation.|Voluminous, rheomorphic, rhyolitic ignimbrite.|
9315|Kathleen Ignimbrite|68996|5|Briefly described|p5, p7|Mesoproterozoic|Mesoproterozoic||1071 +/- 5 Ma|Pussy Cat Group|||Flow banded rhyolites.|
9315|Kathleen Ignimbrite|69003|4|Described|p51-52|Mesoproterozoic|Mesoproterozoic|Southern Talbot Sub-basin. c.500m thick.|1071 +/- 5 Ma.|Pussy Cat Group.||Intercalated with Kathleen Ignimbrite.|Flow-banded ignimbrites; intercalated with volcaniclastic rocks and minor amygdaloidal basalt of the Glyde Formation.|
9315|Kathleen Ignimbrite|69009|5|Briefly described|Map Legend|Stenian|Stenian|Bentley Basin.|1071-1047 Ma|Of the Pussy Cat Group.|||Comprises volcaniclastic rhyolite; typically densely welded, flow-banded rheomorphic ignimbrite; locally well developed eutaxitic- and fiamme-textures; local layers rich in quartz and feldspar phenocrysts.|
9315|Kathleen Ignimbrite|69091|5|Briefly described|p71 Fig.4.14|||Talbot Sub-basin||Pussy Cat Group||||
9315|Kathleen Ignimbrite|69153|5|Briefly described|GEOL_LUT_CSV files; Rocks.csv|Mesoproterozoic|Mesoproterozoic|Bentley Basin, Paterson Orogen. Sample description includes: felsic volcaniclastic rock; rhyolitic rheoignimbrite; granular to porphyritic, rhyolitic pyroclastic rock with a sandstone-like appearance. See file: GEOCHRON/195723.1.pdf, unit sampled is a rhyolitic ignimbrite.|1071 +/- 5 Ma SHRIMP magmatic crystallization age|Pussy Cat Group|||Volcaniclastic rhyolite; typically rheomorphic ignimbrite; locally crystal-rich, lapilli-ash tuff; locally abundant relict glass shards|
9315|Kathleen Ignimbrite|69729|6|Mentioned|p82|||Bedrock of Talbot Sub-basin.||Pussy Cat Group.||||
9315|Kathleen Ignimbrite|70095|5|Briefly described|p16-17,19,22|||Geological province: Musgrave Province. Of Talbot Sub-basin, Bentley Basin. Thickness of rhyolitic package: 0.5km. Strike length: ~35km, interpreted volume of 525km3.||Unit of Pussy Cat Group.||Underlain by Kaarnka Group.||
9315|Kathleen Ignimbrite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP ages derived from sample (195031.1.pdf)|1047 Ma - 1077 Ma (Inferred) 1076 Ma  (SHRIMP)|Pussy Cat Group|||Volcaniclastic rhyolite; typically densely welded, flow-banded rheomorphic ignimbrite, locally well developed eutaxitic and fiamme textures. Volcaniclastic rhyolite; fine-coarse grained, locally crystal rich, lapilli-ash tuff.|
9315|Kathleen Ignimbrite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 195001 (porphyritic rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1062+\-8 Ma. Sample GSWA 195031 (porphyritic rhyolite) yielded an interpreted (regression intersecting concordia curve) magmatic crystallisation age of 1076+\-8 Ma. Sample GSWA 195058 (porphyritic rhyolite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1078+\-5 Ma. Sample GSWA 195723 (rhyolitic ignimbrite) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1071+\-5 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Volcaniclastic rhyolite; typically densely welded, local lapilli-ash tuff, flow-banded rheomorphic ignimbrite.|
9315|Kathleen Ignimbrite|71211|4|Described|i-iv, vii, x, xiii, xiv, p1-p3|Mesoproterozoic|Mesoproterozoic|West Musgrave Province. Less than 650m thick volcano-sedimentary sequence. Deposited in a marine shelf or lacustrine environment as an intra-caldera deposit. Up to 40km2 preserved outcrop that forms the prominent Whitby Range. Referred to repeatedly by the acronym KI throughtout the text. Also referred to as the Kathleen Ignimbrite Formation on p61, p81-p83, p88, p100, p165. Ignimbrites of this formation contain well-preserved volcanic features such as columnar jointing, eutaxitic fiamme, auto breccias, peperite and hyaloclastites. Petrographic description given in detail. On the basis of geochemistry this unit is interpreted to be the most evolved component of a magmatic system that includes the primitive Rowland Suite and the even more primitive Alcurra Dolerite Suite. See also p13, p21-p26,  p27 fig 2.3, p28-p30, p36-p37, p47, p50, p54, p59-p64, p67-p68, p81-p83, p86-p90, p94, p96-p101, p103, p104, p106, p108 fig 3.11, p111-p113, p115-p118, p120, p133-p137, p138, p143-p145, p147-p156, p159-p166, p178-p179, p182-p183, p197, p207, p209-p210, p213, p216-p218, p243, p249, p253, p261, p270-p271.|1071 +/- 5 Ma|Pussy Cat Group|Includes the Kurrparu Member, Karlaya Member and the Kilykilykarri Member.|Overlies the Cleghorne Formation. Intruded by the Rowland Suite.|Rhyolitic, ignimbrite dominated volcanic sequence.|
9315|Kathleen Ignimbrite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite, ignimbirte|
9315|Kathleen Ignimbrite|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). Samples GSWA 195001, 195031 and 195058 (porphyritic rhyolites) yielded concordia ages of 1062+\-8, 1076+\-8 and 1078+\-5 Ma, interpreted as mean magmatic crystallisation ages of the rhyolite samples. Sample GSWA 195723 (rhyolitic ignimbrite) yielded a concordia age of 1071+\-5 Ma, interpreted as magmatic crystallisation age of the ignimbrite. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1077-1047 Ma (inferred)|Unit of Pussy Cat Group.|||Volcaniclastic rhyolite; fine- to coarse-grained, locally crystal-rich, lapilli-ash tuff; locally abundant relict glass shards; flow-banded rheomorphic ignimbrite.|
9315|Kathleen Ignimbrite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1071+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Coarse-grained crystal-rich quartz- and feldspar- rhyolite; feldspar-dominated fragmental porphyritic rhyolite.|
9315|Kathleen Ignimbrite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Pussy Cat Group|||Volcaniclastic rhyolite.|
9315|Kathleen Ignimbrite|72443|6|Mentioned|p738, p740, p742-743, p756|||Locally over 500m thick.|1050 +/- 18 Ma to 1071 +/- 6 Ma (SHRIMP U-Pb)|Pussy Cat Group|||Primarily flow-banded and lava-like rheomorphic ignimbrite.|
9317|Kathleen Valley Gabbro|7471|6|Mentioned|p20.|||Kathleen Valley area, Agnew-Wiluna belt. Minor Cu mineralisation in pyrite-chalcopyrite-quartz veins, commonly with Au and Ag, is found in mafic hosts spatially related to NNW-trending shear zones in this unit.||||||
9317|Kathleen Valley Gabbro|23209|6|Mentioned|p7 Fig.13|||||||||
9317|Kathleen Valley Gabbro|23281|6|Mentioned|p5|||||||||
9317|Kathleen Valley Gabbro|23595|4|Described|p10|||Overlain by Mount Goode Basalt. Geological Province: Yilgarn Craton.||||||30-SEP-08
9317|Kathleen Valley Gabbro|23611|6|Mentioned|p24|||||||||
9317|Kathleen Valley Gabbro|24135|3|Fully described|p13|Archean|Archean|Age: 2736+/-3Ma (SHRIMP U-Pb).  Previously Kathleen Valley gabbro and Kathleen Valley Granophyre.||||||07-NOV-08
9317|Kathleen Valley Gabbro|24174|5|Briefly described|p4, p6, p34|Archean|Archean|Geological Province: Eastern Goldfields.||||||07-NOV-08
9317|Kathleen Valley Gabbro|24196|5|Briefly described|p18, p51|Archean|Archean|Age: 2.736 Ga (Black et al., 2002). Geological Province: Yilgarn Craton||||||07-NOV-08
9317|Kathleen Valley Gabbro|35113|6|Mentioned|p42|||||||||
9317|Kathleen Valley Gabbro|38497|5|Briefly described|p53|||||||||
9317|Kathleen Valley Gabbro|38514|6|Mentioned|Fig.5|||||||||
9317|Kathleen Valley Gabbro|38765|6|Mentioned|p100|||||||||
9317|Kathleen Valley Gabbro|43288|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
9317|Kathleen Valley Gabbro|44149|6|Mentioned|p102|Archean|Archean|Appears as Kathleen Valley gabbro.||||||
9317|Kathleen Valley Gabbro|44924|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
9317|Kathleen Valley Gabbro|64586|5|Briefly described|Map legend|Archean|Archean|Undivided gabbro; anorthositic gabbro and anorthosite; quartz gabbro and tonalite and pyroxene-rich gabbro - all metamorphosed.||||||23-DEC-09
9317|Kathleen Valley Gabbro|65200|6|Mentioned|Map legend|Archean|Archean|Gabbro. Of the Yilgarn Craton. Only shown on simplified geology [solid geology?] inset map.||||||24-NOV-09
9317|Kathleen Valley Gabbro|66195|5|Briefly described|p610, p611 Fig.9|Neoarchean||Southern Cross Domain,  Youanmi Terrane.|2736 +/ -3 Ma.|||||13-MAR-12
9317|Kathleen Valley Gabbro|66880|6|Mentioned|p8. |Archean|Archean|Yackabindie Domain, Agnew-Wiluna Belt. |2735 +/- 3 Ma (Black et al. 2002).|||||
9317|Kathleen Valley Gabbro|67129|5|Briefly described|p55|Archean|Archean|Southern Cross Domain, Youanmi Terrane.|2736 +/- 3 Ma.|||||
9317|Kathleen Valley Gabbro|68107|6|Mentioned|p618|Neoarchean|Neoarchean|Eastern Youanmi Terrane.|ca. 2736 +/- 3 Ma (Liu 2007).|||||
9317|Kathleen Valley Gabbro|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Eastern Goldfields Superterrane, Yilgarn Craton|||Includes 6 unnamed subunits.||Quartz gabbro and tonalite; anorthositic gabbro and anorthosite; gabbro; pyroxene-rich gabbro; layered gabbro with rhythmic layering (2-10 cm) due to varying proportions of amphibole and plagioclase; all metamorphosed.|06-AUG-15
9317|Kathleen Valley Gabbro|69414|6|Mentioned|p86, 88|Archean|Archean|Yakabindie Domain, Yilgarn Craton.|2736 +/- 3 Ma (Liu et al., 2002).||||Includes a tonalite intrusion.|
9317|Kathleen Valley Gabbro|69617|6|Mentioned|p154|||Liu et al. (2002).||||||
9317|Kathleen Valley Gabbro|70153|5|Briefly described|100k_geologyp10_lut.csv|Neoarchean|Neoarchean|See also 500k_interpgeop14_lut.csv.|2735 Ma (inferred).||||Quartz and anorthositic gabbros, tonalite, anorthosite. Quartz gabbro and pyroxene-rich gabbro. Layered gabbro with rhythmic layering (2-10 cm) due to varying proportions of amphibole and plagioclase; metamorphosed.|
9317|Kathleen Valley Gabbro|70276|6|Mentioned|p783|||Yackabindie Domain, Agnew-Wiluna greenstone belt.|2735 +/- 3 Ma (Black et al., 2002).|||||
9317|Kathleen Valley Gabbro|70326|5|Briefly described|p360|Neoarchean|Neoarchean|Geological province: Boorara Domain North, Kalgoorlie Terrane, Yilgarn Craton. Tonalite from Kathleen Valley Gabbro, U-Pb zircon, SHRIMP (Black et al., 2002).|2736+\-3 Ma (Black et al., 2002).|||Overlain by McFarlanes Basalt.||
9317|Kathleen Valley Gabbro|70830|5|Briefly described|p27-p28|||Southern Cross Domain.||||||
9317|Kathleen Valley Gabbro|71168|5|Briefly described|p7|Neoarchean|Neoarchean|Murchison Domain, Youanmi Terrane, Yilgarn Craton.||||||
9317|Kathleen Valley Gabbro|71212|5|Briefly described|p89, p239, p247|Neoarchean|Mesoarchean|Yilgarn Craton. Potentially equivalent to the Lawlers greenstones. Also referred to by the informal Kathleen Valley gabbro on p247.  Age is U-Pb zircon from Cooper and Dong, 1983.|2795 +/- 38 Ma |||Unconformably overlain by the Jones Creek Conglomerate.||
9317|Kathleen Valley Gabbro|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Neoarchean|Geological province: Eastern Goldfields Superterrane, Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma); Eastern Goldfields Superterrane events (2960 - 2600 Ma). See 100k_geologyp10_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|2735 Ma (inferred)||||Gabbro; pyroxene rich and quartz gabbro; metamorphosed; anorthositic gabbro and anorthosite; metamorphosed; tonalite.|
9317|Kathleen Valley Gabbro|71310|4|Described|p778-780, p783-784, p787, p789-790|||Kathleen Valley-Yankabindie district. Source of some clasts in Jones Creek Conglomerate. Faces SE; is overturned. Folding described.|2736 +/- 3 Ma (SHRIMP U-Pb, Black et al., 2002).|||Is overlain unconformably by Jones Creek Conglomerate.|Very coarse-grained anorthosite, gabbro, and tonalite (representing the upper contact differentiate). Includes plagioclase-phyric pillow basalt.|
9317|Kathleen Valley Gabbro|72034|5|Briefly described|500k_interpgeop16_lut|Neoarchean|Neoarchean||||||Gabbro, quartz gabbro, and pyroxenitic gabbro; minor anorthosite and tonalite; metamorphosed.|
9317|Kathleen Valley Gabbro|72049|6|Mentioned|p258|||Metavolcanic basement of the Kalgoorlie Terrane.|2736 +/- 3 Ma (Liu et al, 2002)|||||
9317|Kathleen Valley Gabbro|73596|6|Mentioned|p1160, 1167, 1170|Neoarchean|Neoarchean|Agnew-Wiluna Greenstone Belt, Kalgoorlie Terrane. Subaqueous rift-proximal felsic lava domes and cryptodomes. Presented as KV Gabbro on p1170.|2735 +/- 3 Ma.|||||
9324|Kathwai Member|30565|6|Mentioned|p117|||||||||
9324|Kathwai Member|32164|6|Mentioned|p488|||||||||
9343|Kauring Laterite|42280|6|Mentioned|p53|||||||||
9368|Keep Inlet Formation|13194|4|Described|p388 Tb. 4-16; p382, 405 figs 4-59,-71|Asselian|Gzhelian|Type Section: 3.5km NE of Cleanskin Bore: 15o03'S 128o58'E. Reference section: Keep River 1 well (0-480m).  Up to 480m thick fan delta, fluvial and glacio-marine deposits.||Kulshill Group||Overlies Weaber Group and Langfield Group (both unconformably).|Sandstone, pebbly sandstone, mudstone, conglomerate, tillite; minor coal.|
9368|Keep Inlet Formation|22814|5|Briefly described|fig2|Permian|Permian|||||||
9368|Keep Inlet Formation|23858|5|Briefly described|p920|Permian|Carboniferous|Geological Province: Bonaparte Basin. Max. thickness: 480 m||||||
9368|Keep Inlet Formation|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Kulshill Group.  Deltaic sandstone, pebbly sandstone, mudstone and minor coal.  Geological Province: Bonaparte Basin.||||||
9368|Keep Inlet Formation|24569|5|Briefly described|p248 Fig. 3|Early Permian|Early Permian|Age: ~295Ma. Geological Province: Petrel Sub-basin.||||||
9368|Keep Inlet Formation|40993|6|Mentioned|p10|||||||||
9368|Keep Inlet Formation|41532|5|Briefly described|p297|||||||||
9368|Keep Inlet Formation|41598|6|Mentioned|p412|||||||||
9368|Keep Inlet Formation|41839|4|Described|p32|||Formerly "Keep Inlet Beds".||||||04-OCT-06
9368|Keep Inlet Formation|41864|3|Fully described|p145|||Equivalent to Kulshill Formation of NT and offshore. Also mentioned p108.||||||04-OCT-06
9368|Keep Inlet Formation|41865|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||||||
9368|Keep Inlet Formation|42442|5|Briefly described|p13|||||||||
9368|Keep Inlet Formation|42547|5|Briefly described|p103|||||||||
9368|Keep Inlet Formation|42734|5|Briefly described|map legend|Permian||||||||
9368|Keep Inlet Formation|43236|5|Briefly described|p14|Early Permian|Late Carboniferous|Bonaparte Basin. Formerly "Keep Inlet Beds".||||||
9368|Keep Inlet Formation|60682|5|Briefly described|p25 Fig. 22|Asselian|Stephanian|Of Kushill Group. Overlain by Keyling Formation. Partially laterally equivalent to Kuriyippi Formation. Sandstone. Geological Province: Bonaparte Basin.||||||
9368|Keep Inlet Formation|64580|4|Described|map legend||Early Permian|Of Kulshill Group. Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene.||||||09-DEC-08
9368|Keep Inlet Formation|64630|6|Mentioned|p38|||Of Kushill Group.||||||
9368|Keep Inlet Formation|67354|5|Briefly described|p73. |||Type locality north of Cleanskin Bore at 22/6.||Onshore unit in Kulshill Group.|||Light grey, feldspathic calcareous quartz sandstones with clay clasts, pebbles and boulders to 2m consisting of schist, slate, quartzite, gneiss, granite and glauconitic limestone; striated.|
9368|Keep Inlet Formation|69099|5|Briefly described|500k_geologyp08_lut.csv||Early Permian|||Kulshill Group|||Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene.|31-JUL-15
9368|Keep Inlet Formation|69165|4|Described|500k_geologyp08_lut.csv|Permian|Permian|||Kulshill Group|||Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene.|
9368|Keep Inlet Formation|69418|5|Briefly described|p3:34|Permian|Permian|Onshore Bonaparte Basin. Coal was recognised in this unit prior to 1894.||||||12-JUL-16
9368|Keep Inlet Formation|69452|4|Described|p36:9, 12, 14, 18, 25-26|||Cockbain (1985); equivalent to Keep Inlet Beds of Veevers and Roberts (1968). Subsurface. Onshore Keep Inlet Sub-basin, Bonaparte Basin. Fluvial and fan delta, glacigenic deposits. Up to 480m thick. Poorly dated; relationships to other Formations in the Group are uncertain. Spores and palynomorphs, and the interpreted glacigenic environment of deposition, indicate a likely correlation with upper Kuriyippi to basal Quoin Formations. Coal beds up to 3m thick were intersected in Keep River-1 drillhole.||Kulshill Group.||Unconformably overlies Septimus Limestone (Langfield Group).|Calcareous, feldspathic and lithic quartz sandstone, with clay clasts, and pebbles and boulders of exotic rocks; minor coal.|12-JUL-16
9368|Keep Inlet Formation|69634|5|Briefly described|500k_geologyp08_lut.csv||Early Permian|||Unit of Kulshill Group.|||Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene|
9368|Keep Inlet Formation|69673|4|Described|p173|||||Kulshill Group|||Calcareous, feldspathic and lithic quartz sandstone with clay clasts and pebbles and boulders of exotic rocks; minor coal.|
9368|Keep Inlet Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Sakmarian|Asselian||290-298 Ma||||Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene|
9368|Keep Inlet Formation|70812|6|Mentioned|p7|||||||||
9368|Keep Inlet Formation|70851|6|Mentioned|p17|||||||||
9368|Keep Inlet Formation|71267|4|Described|GEOL_LUT_CSV files|Sakmarian|Asselian|Of Southern Bonaparte Basin. Events: Alice Springs Orogeny (450-295 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|298.9-290.1 Ma (biostrat)|Unit of Kulshill Group.|||Deltaic sandstone, pebbly sandstone, mudstone, conglomerate and minor coal; in part glaciogene.|
9368|Keep Inlet Formation|72034|5|Briefly described|500k_interpgeop16_lut|Sakmarian|Asselian|Southern Bonaparte Basin.  Age from biostratigraphy.||Kulshill Group|||Sandstone, mudstone, conglomerate (including diamictite); minor coal; in part glacigene.|
9384|Keith Kilkenny Greenstones|30440|6|Mentioned|p71|||Age; Geochemistry. See also P78,80,81||||||
9402|Kellys Knob Sandstone|13194|4|Described|p393 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: near Kellys Knob 15o46'S 128o45'E. 70-350m thick eolian, fluvial and tidal deposits.||||Overlies Antrim Plateau Volcanics (unconformably). Overlies and equivalent to Steeple Peak Sandstone and Cyril Sandstone and Ragged Range Conglomerate (all conformably).|Quartz sandstone; rare shale.|
9402|Kellys Knob Sandstone|40792|6|Mentioned|Fig.5|||||||||
9402|Kellys Knob Sandstone|40993|6|Mentioned|p4|||||||||
9402|Kellys Knob Sandstone|41598|5|Briefly described|p413|||Mention p412.||||||04-OCT-06
9402|Kellys Knob Sandstone|41864|3|Fully described|p51|||||||||
9402|Kellys Knob Sandstone|41865|5|Briefly described|Map legend|Frasnian||||||||
9402|Kellys Knob Sandstone|42030|5|Briefly described|p749|||||||||
9402|Kellys Knob Sandstone|42175|5|Briefly described|Fig.2 P200|||||||||
9402|Kellys Knob Sandstone|44230|5|Briefly described|Map Legend||Frasnian|||||||
9402|Kellys Knob Sandstone|60006|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin. Of Cockatoo Group. Quartz sandstone.||||||
9402|Kellys Knob Sandstone|60682|4|Described|p22 Table 5, 23|Devonian|Devonian|Of Cockatoo Group. Previously Kellys Knob Sandstone Member. Overlies Ragged Range Conglomerate, unconformably overlies Whitewater Volcanics and Halls Creek Group. Thickness: >300m. Geological Province: Bonaparte Basin.||||||
9402|Kellys Knob Sandstone|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
9402|Kellys Knob Sandstone|65331|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Cockatoo Group, Bonaparte Basin. Quartz sandstone ||||||
9402|Kellys Knob Sandstone|68473|6|Mentioned|p531|Devonian|Devonian|||||||
9402|Kellys Knob Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
9402|Kellys Knob Sandstone|69452|4|Described|p36:6, 9-10|Frasnian|Frasnian|Rowley and Lee (1986). Equivalent to Kellys Knob Sandstone Member (Veevers and Roberts, 1986). Petrel Sub-basin, Bonaparte Basin. Onshore. Crops out as prominent, deeply dissected plateaux that dominate the topography and are scenic attractions. At least 300m thick. Aeolian, fluvial and tidal deposits. Locally a distal facies equivalent of Ragged Range Conglomerate.||Cockatoo Group.||Conformably overlies and interfingers with Ragged Range Conglomerate. Unconformably overlies Halls Creek Group and Whitewater Volcanics. Is faulted against Enga Sandstone and Burt Range Formation.|Red to orange, tabular, cross-bedded, medium-grained, pebbly quartz sandstone with conglomerate beds towards the base.|12-JUL-16
9402|Kellys Knob Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
9402|Kellys Knob Sandstone|69673|5|Briefly described|p169|||||Cockatoo Group||Overlies Ragged Range Conglomerate, overlain by Cecil Sandstone, unconformably overlain by Buttons Formation|Quartz sandstone with conglomeratic beds.|
9402|Kellys Knob Sandstone|70206|5|Briefly described|Map Legend|Devonian|Devonian|Bonaparte Basin.||Unassigned Cockatoo Group|||Quartz sandstone.|
9402|Kellys Knob Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Cockatoo Group.|||Fine to medium grained quartz sandstone|
9434|Kennedy Group|12466|5|Briefly described|p178.|Permian|Permian|Enderby Terrace, Dampier Sub-basin. No demonstrated hydrocarbon source potential.|||||Sandstones and claystones.|
9434|Kennedy Group|12471|5|Briefly described|p475 Fig.2. |Late Permian|Late Permian|Marine-deltaic sedimentation.||||Overlies Callytharra Formation. Is overlain by Locker Shale.|Includes sandstones and limestones.|
9434|Kennedy Group|12731|6|Mentioned|p591 Fig.3.|||||||Overlies Wooramel Group.||
9434|Kennedy Group|12733|5|Briefly described|p554 Fig.2, pp556-562, p566.|Late Permian|Early Permian|Kungurian-Kazanian. Oil and gas source in Peedamullah Shelf. Hydrocarbon generating potential is fair to excellent, and it is overlain by a thick Triassic-Tertiary section.||||Overlies Byro Group.|Predominantly clastic shallow marine deposits.|
9434|Kennedy Group|13615|5|Briefly described|p3-p4, p6-p8, p12-14, p103 App. 3.|Early Triassic|Late Permian|Peedamullah Shelf. Spores and Pollen zone provided. Mistakenly referred to as the Kennedy Formation on p22. Interpreted by Hocking et al (1987) to have been deposited in a sandy, marine-shelf dominated depositional environment. Intersected in Candace 1 at 1458m. See also  p16-p17, p20, p22, p27, p29-p31, p34-p35, p39, p41-p42, p44-p45, p48-p51, p54-p55, p58-p59, p66-p67, p69, p76, p78-p80, p84, .|c. 274 Ma||Includes the Cody Limestone, Abdul Sandstone and the Chinty Formation.|Unconformably overlies Lyons Group, Callytharra Formation. Conformably overlies Byro Group. Overlain by the Locker Shale.||07-FEB-19
9434|Kennedy Group|14228|5|Briefly described|p5 fig 2, p8, p15, p17-18|Permian|Kungurian|Merlinleigh Sub-basin. Various models for its evolution presented.|||Coolkilya Sandstone, Mungadan Sandstone, Binthalya Formation.|Overlies Byro Group.|Interbedded sandstone and shale.|
9434|Kennedy Group|22814|5|Briefly described|fig2|Permian|Permian|||||||
9434|Kennedy Group|23174|5|Briefly described|Fig5p8||Late Permian|||||||
9434|Kennedy Group|23311|5|Briefly described|map legend||Early Permian|Minimum age poorly constrained - Palaeozoic.||||||
9434|Kennedy Group|23312|5|Briefly described|map legend||Early Permian|||||||
9434|Kennedy Group|23403|4|Described|p8|Late Permian|Middle Devonian|||||||24-NOV-09
9434|Kennedy Group|23620|5|Briefly described|p4 Fig. 4|Permian|Permian|||||||
9434|Kennedy Group|23726|4|Described|p37|Late Permian|Early Permian|Underlying unit Byro Group. Geological Province: Carnarvon Basin.||||||
9434|Kennedy Group|23815|5|Briefly described|p288|||Formerly known as the "Kennedy Stage" or the "Kennedy Sandstone". Geological Province: Carnarvon Basin. Underlying unit: Byro Group (conformable). Includes the Coolkilya Greywack, Mungadan Sandstone and Binthalya Formation.||||||18-APR-05
9434|Kennedy Group|23976|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
9434|Kennedy Group|23977|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
9434|Kennedy Group|23978|5|Briefly described|Map Legend|Phanerozoic|Phanerozoic|||||||
9434|Kennedy Group|24044|2|Defined|p539|Permian|Carboniferous|Formerly Kennedy Sandstone. Geological Province: Merlinleigh Sub-basin.||||||16-NOV-09
9434|Kennedy Group|24059|5|Briefly described|p137|Permian|Permian|Geological Province: Carnarvon Basin.||||||
9434|Kennedy Group|24114|6|Mentioned|p8|||Geological Province: Yilgarn Craton.||||||
9434|Kennedy Group|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
9434|Kennedy Group|29721|6|Mentioned|Table 102|||||||||
9434|Kennedy Group|30545|6|Mentioned|Fig.2|||Permian||||||
9434|Kennedy Group|31561|4|Described|p37|||See also p34. Artinskian - Tatarian||||||18-MAR-20
9434|Kennedy Group|31604|6|Mentioned|p6|||Kungurian. Table 4||||||
9434|Kennedy Group|32163|6|Mentioned|p279|||Stratigraphic column Fig.2||||||
9434|Kennedy Group|32648|6|Mentioned|p32|||Perm.||||||
9434|Kennedy Group|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
9434|Kennedy Group|33386|6|Mentioned|p7|||||||||
9434|Kennedy Group|33450|6|Mentioned|p11|||Fig.5||||||
9434|Kennedy Group|33453|4|Described|p70|||Late Perm. See also P74.||||||
9434|Kennedy Group|33701|6|Mentioned|Fig.1|||Kungurian-Kazanian.||||||
9434|Kennedy Group|33710|6|Mentioned|Table 1|||See also P120.||||||
9434|Kennedy Group|33711|6|Mentioned|p384|||Table 4||||||
9434|Kennedy Group|34008|6|Mentioned|p71|||U.Perm.||||||
9434|Kennedy Group|34009|6|Mentioned|Table III|||||||||
9434|Kennedy Group|34138|6|Mentioned|Cor.Chart|||Kungurian - Kazanian||||||
9434|Kennedy Group|34532|6|Mentioned|p225|||Members of the group||||||
9434|Kennedy Group|34846|6|Mentioned|Fig.3|||||||||
9434|Kennedy Group|35144|6|Mentioned|p4|||||||||
9434|Kennedy Group|35282|6|Mentioned|p3|||See also Fig.2.||||||
9434|Kennedy Group|35983|6|Mentioned|Table 27|||||||||
9434|Kennedy Group|36257|6|Mentioned|Table 2.1|||||||||
9434|Kennedy Group|36740|6|Mentioned|p2|||||||||
9434|Kennedy Group|36890|3|Fully described|p288|||Formerly Kennedy Sandstone,Kennedy Stage.||||||09-DEC-08
9434|Kennedy Group|37294|6|Mentioned|p100|||||||||
9434|Kennedy Group|37295|6|Mentioned|Table 2|||||||||
9434|Kennedy Group|37303|4|Described|p65|||||||||
9434|Kennedy Group|37304|6|Mentioned|p55|||||||||
9434|Kennedy Group|39316|6|Mentioned|Fig.2|||||||||
9434|Kennedy Group|39427|4|Described|Table 1|||||||||
9434|Kennedy Group|40617|6|Mentioned|p5|||Mention Fig.1||||||
9434|Kennedy Group|40992|6|Mentioned|Fig.8|||||||||
9434|Kennedy Group|41158|5|Briefly described|p229|||||||||
9434|Kennedy Group|41170|6|Mentioned|Fig.4|||||||||
9434|Kennedy Group|41172|6|Mentioned|p123|||||||||
9434|Kennedy Group|41271|3|Fully described|p100|||||||||
9434|Kennedy Group|41436|6|Mentioned|p41|||||||||
9434|Kennedy Group|41438|4|Described|p104|||||||||
9434|Kennedy Group|41441|5|Briefly described|p151|||||||||
9434|Kennedy Group|41443|4|Described|p163|||||||||
9434|Kennedy Group|41444|6|Mentioned|Fig.4|||||||||
9434|Kennedy Group|41447|6|Mentioned|Fig.3|||||||||
9434|Kennedy Group|41632|6|Mentioned|p1|||||||||
9434|Kennedy Group|41689|6|Mentioned|Table 1|||||||||
9434|Kennedy Group|42075|5|Briefly described|Fig.4 P245|||||||||
9434|Kennedy Group|42116|5|Briefly described|p27|||See also Fig.11||||||
9434|Kennedy Group|42392|6|Mentioned|p115|||||||||
9434|Kennedy Group|42463|6|Mentioned|Fig.2 P169|||||||||
9434|Kennedy Group|42711|6|Mentioned|p30|||Geological province: Carnarvon Basin.  Shallow marine deposits.||||||
9434|Kennedy Group|43826|6|Mentioned|Fig.2,p163||Late Permian|||||||01-MAR-10
9434|Kennedy Group|44219|14|Not recorded|p31|Kazanian|Kungurian|U.Kungurian-Kazanian.||||||
9434|Kennedy Group|44344|14|Not recorded|p.3,11,15-17|||Includes Coolkilya Greywacke, Mungadan Sandstone & Binthalya Formation (top). (G50-1). opp.4 map.||||||
9434|Kennedy Group|44345|14|Not recorded|map legend||Kungurian|||||||
9434|Kennedy Group|44537|14|Not recorded|map legend||Artinskian|||||||
9434|Kennedy Group|44657|14|Not recorded|p.10|||||||||
9434|Kennedy Group|44994|6|Mentioned|Fig.7|||Correlation.Permian.||||||
9434|Kennedy Group|45001|14|Not recorded|p7|Kungurian|Artinskian|||||||
9434|Kennedy Group|45015|5|Briefly described|p7, map legend|Kungurian|Kungurian|Sandstone unit first described by Maitland (1909?). Probably obsolete name? Included: Coolkilya Greywacke, Mungadan Sandstone and Binthalya Formation. Geological Province: Carnarvon Basin.||||||14-JUN-06
9434|Kennedy Group|45016|2|Defined|p.176-180|Tatarian|Kungurian|Tb. at back, p.125,155,156,174-180. Kungurian-?Tatarian. (G50-1).||||||
9434|Kennedy Group|46849|6|Mentioned|Fig. 6|||||||||
9434|Kennedy Group|48610|14|Not recorded|Pl.1|||||||||
9434|Kennedy Group|48848|14|Not recorded|p.38|||||||||
9434|Kennedy Group|48858|14|Not recorded|p.5-15|||(G50-1/Norton). Pl.2.||||||
9434|Kennedy Group|49644|5|Briefly described|Table|||||||||
9434|Kennedy Group|50620|5|Briefly described|p189|Early Permian|Early Permian|Subdivided into the Coolkilya and Mungadan Sandstones and the Binthalya Formation. Geological Province: Merlinleigh Sub-basin (Carnarvon Basin).||||||
9434|Kennedy Group|60331|5|Briefly described|p33 Fig.2|||Overlies Byro Group. Geological Province: Southern Carnarvon Basin.||||||
9434|Kennedy Group|60384|6|Mentioned|p243 Fig 2b|Permian|Permian|Northern Carnarvon Basin.||||||
9434|Kennedy Group|60386|6|Mentioned|p297|Lopingian|Guadalupian|Carnarvon Basin. Deltaic - nearshore - shelf. Age shown as ~late Permian.||||||
9434|Kennedy Group|60725|5|Briefly described|p29-32; p34; p35-36 Figs.5,6; p39.  |Late Permian|Middle Permian|Peedamullah Shelf. Source beds are within the oil generation window.||||||
9434|Kennedy Group|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Includes: Coolkilya Greywacke, Mungadan Sandstone and Binthalya Formation.||||||21-MAR-06
9434|Kennedy Group|64580|4|Described|map legend|Late Permian|Early Permian|Sandstone, shale, siltstone, claystone; includes COOLKILYA SANDSTONE, MUNGADAN SANDSTONE, and BINTHALYA FORMATION.||||||18-MAR-20
9434|Kennedy Group|64630|5|Briefly described|p31 Fig.2|Roadian|Kungurian|Province: Southern Carnarvon Basin. Overlies the Byro Group. Palynology age: P. sinuosus to D. granulata.||||||24-NOV-09
9434|Kennedy Group|64972|6|Mentioned|p617 Fig. 5|Permian|Permian|||||||
9434|Kennedy Group|64974|5|Briefly described|p147 Fig. 5|Kazanian|Ufimian|Includes Coolkilya and Binthalya Formations and Mungaden Sandstone. Geological Province: Carnarvon Basin.||||||24-JUN-09
9434|Kennedy Group|66189|5|Briefly described|p453-454, p459, Fig 2|Permian|Permian|Contains the Coolkilya and Mungadan Sandstones, and Binthalya Formation. Carnarvon Basin. Near shore and shoreface settings. Cessation of Permian marine deposition is recorded by these units.||||||
9434|Kennedy Group|66949|6|Mentioned|p7|Permian|Permian|Southern Carnarvon Basin. A Kungurian-Roadian age suggested by Mory and Backhouse (1997) is supported by SHRIMP dating of Binthalya Formation by Lever and Fanning (2004).|||Includes Binthalya Formation.|||
9434|Kennedy Group|67200|5|Briefly described|p7 fig 5,|Permian|Permian||||Includes Coolkilya Sandstone, Mungadan Sandstone, Binthalya Sandstone|Overlies Byro Group||
9434|Kennedy Group|67354|6|Mentioned|p72.|Permian|Permian|||||||
9434|Kennedy Group|69011|5|Briefly described|Map Legend|Permian|Permian|Southern Carnarvon Basin.|||Includes Binthalya Formation, Mungadan Sandstone, and Coolkilya Sandstone.||Includes grey to black siltstone and shale; interbedded sandstone; very fine to coarse-grained sandstone (commonly silty); minor siltstone and shale.|
9434|Kennedy Group|69029|5|Briefly described|p323,326,328|Kazanian|Kungurian|Of onshore Carnarvon Basin; Peedamullah Shelf. Contains source rock intervals of excellent to fair quality.||||Underlain by Byro Group.||
9434|Kennedy Group|69166|5|Briefly described|500k_geologyp08_lut.csv|Permian|Permian||||||Sandstone, shale, siltstone, claystone.|
9434|Kennedy Group|69182|5|Briefly described|Ch3 p3, Ch3 p8, Ch3 p11|Permian|Permian|Carnarvon Basin. Maximum thickness greater than 1067m. Deposited in a shallow marine setting. Displays good reservoir characteristics and is sealed by the Locker Shale. See also Ch3 p15, Ch3 p23-p27, Ch3 p29, Ch3 p33-p34, Ch3 p45, Ch3 p50, Ch3 p52, Ch3 p54, Ch3 p58, Ch3 p63.||||Overlies the Lyons Group. Overlain by the Locker Shale.|Carbonates and sandstones.|
9434|Kennedy Group|70774|5|Briefly described|p5 fig 3|Midian|Kungurian|Southern Carnarvon Basin.||||Overlies the Byro Group.||06-FEB-20
9434|Kennedy Group|70795|6|Mentioned|100k_geologyp_lut.csv|Guadalupian|Guadalupian||||Includes Binthalya Formation, Mungadan Sandstone, Coolkilya Sandstone|||
9434|Kennedy Group|70826|6|Mentioned|p6 tbl 3|Permian|Permian|Southern Carnarvon Basin.||||||
9434|Kennedy Group|71146|5|Briefly described|p6, p41|Guadalupian|Kungurian|Southern Carnarvon Basin.||||Overlies the Byro Group.|Sandstone.|
9434|Kennedy Group|71623|5|Briefly described|p345, 346 fig 2|Kungurian|Kungurian|Carnarvon Basin|||Includes Chinty Formation, Cody Formation.||Sandstone|
9434|Kennedy Group|72034|5|Briefly described|500k_interpgeop16_lut|Guadalupian|Roadian|Southern Carnarvon Basin. Max  age from biostratigraphy, min age inferred.|||||Sandstone, shale, siltstone, claystone.|
9434|Kennedy Group|72505|5|Briefly described|p890|Wordian|Roadian|Southern Carnarvon Basin. Correlates with the Praecolpatites sinuosus zone and the Dulhuntyispora granulata zone.|||Includes the Coolkillya Sandstone, Mungadan Sandstone and the Binthalya Formation.|Overlies the Byro Group.||
9434|Kennedy Group|72910|4|Described|p1, p4, p6-7, p11-14, p17-20, p25.|Capitainian|Kungurian|Thickness 200-1000m. Recognised in Merlinleigh Sub-basin and Peedamullah Shelf. Includes  sandstone, limestone and claystone previously assigned to the Byro Group. Apparently diachronous, younger on Peedamullah Shelf. Intersected  in Kennedy Range 1 well which contains a complete section of this group. See also p38-39, p41.|||Includes Chinty Formation, Binthalya Formation, Mungadan Sandstone and Coolkilya Sandstone.|Conformably overlies Byro Group. Disconformably overlies Lyons Group,  Callytharra Formation. Overlain by Locker Shale.|Sandstone with lesser siltstone, shale and limestone and interbedded sandstone and siltstone.|18-FEB-21
9434|Kennedy Group|73623|5|Briefly described|p4|Guadalupian|Guadalupian|Merlinleigh Basin.||||Overlies Byro Group. Correlative of Wagina Sandstone.||
9450|Keogh Formation|22817|4|Described|p4|||||||||
9450|Keogh Formation|23174|5|Briefly described|Fig5p8|Permian|Permian|||||||
9450|Keogh Formation|23569|4|Described|p4 Tb. 1|Early Permian|Early Permian|Parent: Wooramel Group.   Siltstone, sandstone, minor claystone, and carbonaceous shale||||||
9450|Keogh Formation|23726|6|Mentioned|p12|||Geological Province: Carnarvon Basin.||||||
9450|Keogh Formation|23815|4|Described|p283|Artinskian|Artinskian|Geological Province: Carnarvon Basin. Underlying unit: One Gum Formation (conformable). Overliying unit: Madeline Formation (conformable). Max. thickness: 73 m. Fossiliferous.||||||
9450|Keogh Formation|24044|5|Briefly described|p541 Fig.2|Early Permian|Early Permian|Of Wooramel Group.||||||
9450|Keogh Formation|24114|5|Briefly described|p8|||Of Wooramel Group. Geological Province: Carnarvon Basin.||||||
9450|Keogh Formation|24410|5|Briefly described|p137|Permian|Permian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||24-NOV-09
9450|Keogh Formation|32113|6|Mentioned|p52|||||||||
9450|Keogh Formation|32648|6|Mentioned|p32|||Wooramel Gp.||||||
9450|Keogh Formation|33594|6|Mentioned|p37|||||||||
9450|Keogh Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
9450|Keogh Formation|34532|6|Mentioned|p225|||Wooramel Gp.||||||
9450|Keogh Formation|36890|3|Fully described|p283|||||||||
9450|Keogh Formation|37295|6|Mentioned|Table 2|||||||||
9450|Keogh Formation|38493|4|Described|p35|||||||||
9450|Keogh Formation|38494|4|Described|p29|||||||||
9450|Keogh Formation|40336|6|Mentioned|p18|||||||||
9450|Keogh Formation|40339|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
9450|Keogh Formation|40342|6|Mentioned|Map legend|Artinskian|Artinskian|||||||
9450|Keogh Formation|40343|5|Briefly described|p11|||||||||
9450|Keogh Formation|40617|6|Mentioned|Fig.1|||||||||
9450|Keogh Formation|40794|6|Mentioned|p91|||||||||
9450|Keogh Formation|41053|6|Mentioned|Fig.2|||||||||
9450|Keogh Formation|41271|3|Fully described|p88|||||||||
9450|Keogh Formation|41438|6|Mentioned|p104|||||||||
9450|Keogh Formation|42116|4|Described|p27|||||||||
9450|Keogh Formation|42183|6|Mentioned|p360|||||||||
9450|Keogh Formation|42462|6|Mentioned|p55|||||||||
9450|Keogh Formation|43255|5|Briefly described|map legend||Artinskian|of Wooramel Group.||||||
9450|Keogh Formation|43256|5|Briefly described|18,22||Permian|||||||24-NOV-09
9450|Keogh Formation|43835|5|Briefly described|Map Legend||Artinskian|||||||
9450|Keogh Formation|44217|14|Not recorded|Fig.3|||||||||
9450|Keogh Formation|44532|4|Described|p.6,7, map|||(G50-5).||||||
9450|Keogh Formation|44533|5|Briefly described|map legend||Artinskian|Artinskian.||||||
9450|Keogh Formation|44994|6|Mentioned|Fig.7|||Permian.||||||
9450|Keogh Formation|45001|14|Not recorded|p146|||Compared with Carynginia Formation.||||||
9450|Keogh Formation|45015|5|Briefly described|map legend|Artinskian|Artinskian|Of the Wooramel Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
9450|Keogh Formation|45016|2|Defined|p116-121||Artinskian|Tb, p58,74,75,77,91,97,102-7,109,113-4,124,129,145,146. (G50-6,10).||||||
9450|Keogh Formation|48885|14|Not recorded|p.1,2,5,9,10,11-17||Early Permian|Lower Permian (Sakmarian-Artinskian). (G/50-6).||||||
9450|Keogh Formation|61958|5|Briefly described|Map sheet 1|Artinskian|Artinskian|Of the Wooramel Group.||||||
9450|Keogh Formation|64972|5|Briefly described|p620|||Of Wooramel Group. Contains coals. Geological Province: Carnarvon Basin.||||||
9450|Keogh Formation|67195|5|Briefly described|Appendix 2|||Carnarvon Basin.|||||Includes medium-grained to granule sandstone; common cross beds.|
9450|Keogh Formation|67200|5|Briefly described|p18 table 1, p46, p50, app 2 p5|||Thermal conductivity of 2.93 W/mK||Wooramel Group|||Medium grained to granule sandstone with common cross bedding.|
9450|Keogh Formation|67977|5|Briefly described|p481 Fig. 2, p482 Fig. 3|Artinskian|Artinskian|Geol. Prov: Byro Sub-basin, Southern Carnarvon Basin||Wooramel Group||overlies Callytharra Formation|sandstone|
9450|Keogh Formation|69583|6|Mentioned|p133, p134 Fig.3, p135, Plate 4|Permian|Permian|Hosts small coal deposits in a limited distribution area. Seismic interpretation.||||||
9450|Keogh Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, conglomerate, shale, sandstone|
9450|Keogh Formation|72910|4|Described|p4, p16, p20, p22-23, p39, p41-42.|Artinskian|Artinskian|Thickness c. 50m. Restricted to the Byro Sub-basin. Type section: Keough Hill, Southern Byro Plains 25d51m30sS; 115d54m30sE. Sparse fuana and flora. The lower part is interpreted as having been deposited in a tidally influenced delta-plain environment; other outcrop is interpreted to have been deposited in an interdistributary bay environment.||Wooramel Group||Conformably overlies Callytharra Formation and underlies Byro Group and laterally equaivalent to Moogooloo Sandstone, Billidee Formation.|Silty fine to coarse-grained sandstone, lesser clayey siltstone, pebble conglomerate.|18-FEB-21
9462|Keraudren Formation|13255|5|Briefly described|p369, p376|Late Triassic|Late Permian|Roebuck Basin. See also reference to Lower Keraudren Formation (p376).|||Includes Cossigny Member.|Overlies Locker Shale. Is overlain unconformably by Bedout Formation.|Deltaic sands.|29-SEP-15
9462|Keraudren Formation|41438|4|Described|p105|||||||||
9462|Keraudren Formation|41732|6|Mentioned|p534|||See also Fig.3||||||
9462|Keraudren Formation|42615|5|Briefly described|p6|||Triassic||||||
9462|Keraudren Formation|43173|6|Mentioned|12-54||Triassic|||||||
9462|Keraudren Formation|44143|4|Described|p.434 Table 4-19, p447|Triassic|Triassic|>1000m thick; sandstone with minor shale and coal; fluvial. Conformably overlies Locker Shale. Is equivalent to Mungaroo Formation of the Carnarvon Basin. Anisian to Norian.||||||
9462|Keraudren Formation|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Middle Triassic|Age: ~235Ma. Geological Province: Rankin Platform, Beagle Sub-basin and Bedout Sub-basin (Roebuck Basin).||||||01-MAR-10
9462|Keraudren Formation|63929|6|Mentioned|p131 Fig.2.|Triassic|Triassic|Offshore Canning Basin. Predominantly non-marine clastic sediments.||||Overlies Locker Shale.||
9462|Keraudren Formation|66124|4|Described|p169, p171 Fig.2|Rhaetian|Anisian|Middle to Late Triassic. Offshore Canning Basin. Mixed lithology clastic unit. Sometimes referred to as Mungaroo Formation. Non-marine, maximum 200m thick. Overlies Locker Shale.||||||
9462|Keraudren Formation|69297|6|Mentioned|p339, p352|Triassic|Triassic|Misspelt as the Keruadren Formation on p339. Contains potential hydrocarbon reservoir sandstone.  |||Includes the Cossigny Member.|||
9462|Keraudren Formation|69689|6|Mentioned|p16|Triassic|Triassic|Roebuck Basin.||||||
9462|Keraudren Formation|70065|5|Briefly described|Rowley: p2. Regional: p3, p6|Triassic|Triassic|Sandstones form reservoirs.|||Cossigny Member.|Overlies Locker Shale or Poole Sandstone. Is overlain by Bedout Formation.||
9483|Keyling Formation|12466|5|Briefly described|p177 Fig.10.|Early Permian|Early Permian|Rock-Eval data confirm that gas and oil-prone source rocks occur in this unit.||||Overlies Treachery Shale. Is overlain by Fossil Head Formation.||03-SEP-14
9483|Keyling Formation|12733|6|Mentioned|p565.|Early Permian|Early Permian|Bonaparte Basin. Gas-prone.||||||
9483|Keyling Formation|13194|6|Mentioned|p388 Tb.4-16; p382,405 figs 4-59,-71|Artinskian|Asselian|Type Section: Kulshill 1 well (254-1094m). 327-973m thick periglacial fluvial to marginal marine deposits.||Kulshill Group||Overlies Treachery Shale. Overlain by Fossil Head Formation.|Sandstone, silty and carbonaceous shale; minor coal and limestone.|
9483|Keyling Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kulshill Group.||||
9483|Keyling Formation|13234|6|Mentioned|p250 Fig.2,p256, p262 Tb.3,p265.|Permian|Permian|Potential reservoir.||||Overlies Treachery Shale.||
9483|Keyling Formation|13354|6|Mentioned|p376 Fig.7.|Early Permian|Early Permian|Bonaparte Basin. Overlies Treachery Shale and underlies Fossil Head Formation of the Kinmore Group.||99||||28-OCT-14
9483|Keyling Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Permian|||||||01-MAR-10
9483|Keyling Formation|23356|5|Briefly described|26 Tab.2|Early Permian|Early Permian|||||||
9483|Keyling Formation|23377|6|Mentioned|p212 Fig.5||Early Permian|Of Vulcan Sub-basin.||||||04-OCT-06
9483|Keyling Formation|24378|5|Briefly described|p14|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
9483|Keyling Formation|24390|5|Briefly described|p3 Table 1|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
9483|Keyling Formation|24569|5|Briefly described|p248 Fig. 3|Early Permian|Early Permian|Of the Kulshill Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
9483|Keyling Formation|41459|6|Mentioned|Fig.2|||Reserved as Keyling Member.||||||04-OCT-06
9483|Keyling Formation|41532|2|Defined|p300|Early Permian||||||||
9483|Keyling Formation|41731|6|Mentioned|Fig.3|||||||||
9483|Keyling Formation|42055|4|Described|Fig.1 P52|||||||||
9483|Keyling Formation|42442|2|Defined|p16|Sakmarian|Asselian|Variation of Keyling Formation, WA.||||||
9483|Keyling Formation|43482|6|Mentioned|22||Early Permian|||||||
9483|Keyling Formation|43661|6|Mentioned|Fig.3|||||||||
9483|Keyling Formation|43739|6|Mentioned|Fig.5,p38||Early Permian|||||||
9483|Keyling Formation|50085|5|Briefly described|p3 Tb. 1|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
9483|Keyling Formation|60386|5|Briefly described|p297, 309|Artinskian|Artinskian|Petrel Sub-basin, Roebuck/Canning Basin. Deltaic - nearshore - shelf.  ||||||
9483|Keyling Formation|60666|5|Briefly described|p15 (Fig.)|||Geological Province: Bonaparte  Basin.||||||
9483|Keyling Formation|60682|5|Briefly described|p25 Fig. 22||Westphalian|Of Kushill Group. Overlies Treachery Shale and Keep Inlet Formation. Geological Province: Bonaparte Basin.||||||04-OCT-06
9483|Keyling Formation|60701|5|Briefly described|p12, p13|Early Permian|Early Permian|Contains carbonaceous shales and coals; oil reservoirs.  Geological Province: Bonaparte Basin.||||||13-JAN-05
9483|Keyling Formation|62837|5|Briefly described|Stratigraphic columns|Early Permian|Late Carboniferous|Of the Kulshill Group.  Age: ~297-~287Ma. Geological Province:  Western Bonaparte Basin, Petrel Sub-basin (offshore) and Arafura and Money Shoals Basins.||||||01-MAR-10
9483|Keyling Formation|64630|5|Briefly described|p31 Fig.2, p37, p38|Artinskian|Sakmarian|Province: Bonaparte Basin. Part of the Kulshill Group, underlies the Fossil Head Formation, overlies the Treachery Shale.  Palynology age: P. confluens to D. Byroensis. Lithology: dominantly fluvial.||||||24-NOV-09
9483|Keyling Formation|64689|6|Mentioned|p14|Early Permian|Early Permian|These oil source rocks may extend across the Londonderry High, facilitating a widespread Permian oil play.||||||
9483|Keyling Formation|64694|6|Mentioned|p231, p235 Fig.3, p240 Tb.2, p245 Fig.9|Early Permian|Early Permian|Five samples of oil-stained sandstones of this unit were analysed in this study.||||Overlies Treachery Shale. Is overlain by Fossil Head Formation.||
9483|Keyling Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes sandstone, oil impregnated; no non oil sands in core; heterolithic dark grey siltstone/light grey sandstone; whispy siltstone.|23-DEC-22
9483|Keyling Formation|67200|5|Briefly described|app 2 p8||||||||Oil impregnated sandstone.|
9483|Keyling Formation|67354|1|Redefined|p73, pp98-100, p104.|||Redefined. Formerly defined by Mory (1991) with type section between 254 m and 1,094 m in Kulshill-1. Now subdivided into Keyling, Ditji and Quoin Formations. A reference section is erected in Blacktip-1 (2,152.5 - 2,601.5 m). Thickness to c.525 m. Probably deposited in a tidal environment, or meandering stream with subordinate lacustrine facies and coal swamps. It is the primary reservoir target below the regional Fossil Head Formation seal.||Topmost offshore unit in Kulshill Group.||Overlies, probably unconformably, Ditji Formation. Is overlain unconformably to conformably (in the north) by Fossil Head Formation.|Mainly sandstone; lesser siltstone, shale, coal, conglomerate; very minor limestone.|
9483|Keyling Formation|69451|6|Mentioned|p35:9|||Bonaparte Basin. Correlated with part of the Kulshill Group equivalent rocks in the Arafura Basin.||||||12-JUL-16
9483|Keyling Formation|69452|4|Described|p36:8, 11, 15, 18-19, 28|Sakmarian|Sakmarian|Mory (1991); redefined Gorter et al. (2008). Petrel Sub-basin, Bonaparte Basin. Fluvial, subordinate lacustrine and paludal deposits; lesser marginal marine and intertidal. Up to 500m thick. Offshore and onshore. Coaly shales have some oil potential.||Kulshill Group.||Overlies Ditji Formation, probably unconformably. Is overlain by Fossil Head Formation unconformably to conformably (in north).|Mostly sandstone, with lesser siltstone, shale, coal, conglomerate and minor limestone.|12-JUL-16
9483|Keyling Formation|69454|5|Briefly described|p38:4|Sakmarian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kulshill Group.||||12-JUL-16
9483|Keyling Formation|69653|6|Mentioned|p10, 15|Cisuralian|Cisuralian|Petrel Sub-basin.||Kulshill Group.||Overlies Ditji Formation. Is overlain by Fossil Head Formation (Kinmore Group).||
9483|Keyling Formation|69673|5|Briefly described|p168 fig 142, p170 fig 142, p173|Permian|Carboniferous|Reservoir potential.||Kulshill Group||Overlain by Fossil Head Formation, overlies Ditji Formation|Sandstone with lesser siltstone, shale, coal, conglomerate and minor limestone.|
9483|Keyling Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3, p2-4|Sakmarian|Sakmarian|See also Regional geology: Fig.8, p8-9, p11, p13. Hydrocarbon source and reservoir. Sealed by overlying Fossil Head Formation.||Kulshill Group.||Overlies Ditji Formation. Is overlain by Fossil Head Formation.|Includes fluvial shales and coaly shales.|12-JUL-16
9483|Keyling Formation|70774|5|Briefly described|p5 fig 3|Artinskian|Sakmarian|Bonaparte Basin.||||Overlies the Treachery Shale. Overlain by the Fossil Head Formation.||
9483|Keyling Formation|71146|6|Mentioned|p44|||Southern Bonaparte Basin.||Kulshill Group||||
9483|Keyling Formation|72505|5|Briefly described|p890|Artinskian|Sakmarian|Southern Bonaparte Basin. Correlated with the Pseudoreticulaspora pseudoreticulata to the Stratopodocarpites fusus zones.||||Overlies the Ditji Formation. Overlain by the Fossil Head Formation and unconformably by the Flat Top Limestone.||
9483|Keyling Formation|73117|6|Mentioned|p15|Sakmarian|Asselian|Bonaparte Basin, southern.||Kulshill Group||Underlain by Ditji Formation. Overlain by Fossil Head Formation.||
9506|Kiaka Sandstone Member|36293|6|Mentioned|p66|||Refers Logan & Chase 1961.||||||
9540|Kilba Granite|29845|6|Mentioned|p171|||||||||
9540|Kilba Granite|50425|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gascoyne Province. Of the Boolaloo Supersuite.||||||07-NOV-08
9540|Kilba Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, tonalite|
9540|Kilba Granite|72758|5|Briefly described|p4 Fig.1, p11 Tb.1, p43, p45-46.|||Association with migmatite in country rocks suggests Granite probably derived by anatexis of Morrissey Metamorphic Suite. Said to show contact metamorphic aureole (p46). Shown as Kilba granite p43.||||Intrudes Morrissey Metamorphic Suite.|Medium-grained muscovite-biotite adamellite and granite with marginal prophyritic facies. Includes xenoliths of mica schist country rocks.|
9558|Killaloe Formation|23136|6|Mentioned|p265 Fig.1|||||||||
9558|Killaloe Formation|23786|5|Briefly described|p21|Archean|Archean|Of Black Flag Beds.  Geological Province: Yilgarn Craton.||||||07-NOV-08
9558|Killaloe Formation|30562|4|Described|p7|||Archaean age||||||
9558|Killaloe Formation|30959|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
9558|Killaloe Formation|36869|6|Mentioned|p48|||||||||
9558|Killaloe Formation|41432|5|Briefly described|p13|||||||||
9558|Killaloe Formation|63981|6|Mentioned|p93 Fig.3, |Archean|Archean|SE Kambalda Domain. Kalgoorlie Sequence.|||||Felsic volcanic and volcaniclastic rocks.|
9558|Killaloe Formation|71212|6|Mentioned|p240, p241|||Kambalda region.||||||
9558|Killaloe Formation|72049|5|Briefly described|p256|||Geochronology derived from this publication; a single grain is dated at 2850 Ma.|2667 +/- 6 Ma (SHRIMP U-Pb)|Early Merougil Group||||
9572|Kimberley Group|22440|4|Described|p4,5|Statherian|Statherian|1800Ma||||||
9572|Kimberley Group|22526|6|Mentioned|Fig3 P682||Orosirian|||||||
9572|Kimberley Group|22537|6|Mentioned|34|Proterozoic|Proterozoic|||||||
9572|Kimberley Group|22547|5|Briefly described|p8||Orosirian|Geological province: Kimberley Basin. Age: c. 1800 Ma. Overlies Speewah Group.||||||14-NOV-06
9572|Kimberley Group|22716|5|Briefly described|table4, p232|Orosirian|Orosirian|||||||
9572|Kimberley Group|22754|4|Described|p5 Tb. 1, p10 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1800-1790 Ma. Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|23125|5|Briefly described|Table.1||Proterozoic|||||||
9572|Kimberley Group|23314|6|Mentioned|333|||||||||
9572|Kimberley Group|23323|5|Briefly described|p456 Table 1|||||||||07-FEB-07
9572|Kimberley Group|23360|6|Mentioned|847|||||||||
9572|Kimberley Group|23383|5|Briefly described|p18, p5 Tb. 1|||Comprises King Leopold Sandstone, Carson Volcanics, Warton Sandstone and Elgee Siltstone.  Geological Province: Kimberley Basin.  See also p6 Fig. 3.||||||03-AUG-11
9572|Kimberley Group|23599|6|Mentioned|p16|||Overlying unit Louisa Downs Group||||||
9572|Kimberley Group|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|23621|3|Fully described|p22|Paleoproterozoic|Paleoproterozoic|See also page 10 table 1. Age: ~1800 Ma. Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: c1800 Ma. Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|23722|4|Described|p17|Proterozoic|Proterozoic|Early Proterozoic.   Geological Province: Kimberley Basin||||||
9572|Kimberley Group|23751|4|Described|p20|Paleoproterozoic|Paleoproterozoic|Age: 1800-1790 Ma (SHRIMP U-Pb zircon). Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|24173|3|Fully described|p22, p11 Tb.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Basin. Age: ~1800Ma. Unconformably overlies Koongie Park Formation, Shepherds Bore Plutonic Complex. Northwest of Halls Creek it is disconformable on Speewah Group and intruded by sills of Hart Dolerite.||||||07-NOV-08
9572|Kimberley Group|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1790Ma.  Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|29380|4|Described|Table 2|||||||||
9572|Kimberley Group|29693|6|Mentioned|p100|||||||||
9572|Kimberley Group|29845|6|Mentioned|p115|||||||||
9572|Kimberley Group|29946|6|Mentioned|p253|||||||||
9572|Kimberley Group|30097|6|Mentioned|Fig.54|||Also Tables 23,24||||||
9572|Kimberley Group|30525|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|30533|5|Briefly described|p15|||On Table 3||||||
9572|Kimberley Group|30558|6|Mentioned|p36|||||||||
9572|Kimberley Group|30636|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
9572|Kimberley Group|30892|6|Mentioned|Table 1|||Carpentarian||||||
9572|Kimberley Group|30893|5|Briefly described|p205|||Lithology||||||
9572|Kimberley Group|30894|4|Described|p249|||Carpentarian||||||
9572|Kimberley Group|30895|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|30896|4|Described|p16|||||||||
9572|Kimberley Group|30897|4|Described|p12|||Drainage P7||||||
9572|Kimberley Group|30898|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9572|Kimberley Group|31404|6|Mentioned|p257|||||||||
9572|Kimberley Group|31446|4|Described|p6||Carpentarian|Units. SD51-15,16.||||||
9572|Kimberley Group|31662|6|Mentioned|p255|||||||||
9572|Kimberley Group|32108|6|Mentioned|p231|||||||||
9572|Kimberley Group|32586|6|Mentioned|p113|||||||||
9572|Kimberley Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9572|Kimberley Group|32660|4|Described|Table 3|||||||||
9572|Kimberley Group|32662|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|32663|4|Described|Table 1|||Carpentarian||||||
9572|Kimberley Group|32664|6|Mentioned|Map legend|Carpentarian|Carpentarian|Briefly described in notes||||||
9572|Kimberley Group|32728|6|Mentioned|Fig.3|||||||||
9572|Kimberley Group|33540|6|Mentioned|p890|||||||||
9572|Kimberley Group|33851|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9572|Kimberley Group|34067|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|34115|6|Mentioned|p384|||1800 - 1825 my||||||
9572|Kimberley Group|34137|4|Described|Table 1||Carpentarian|Includes Pentecost Sandstone, Elgee Siltstone, Warton Sandstone, Carson Volcanics and King Leopold Sandstone, Carpentarian.||||||
9572|Kimberley Group|34190|4|Described|Table 1|||||||||
9572|Kimberley Group|34462|4|Described|p8|||See Table 1. Carpentarian||||||
9572|Kimberley Group|34463|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
9572|Kimberley Group|36003|6|Mentioned|p1028|||||||||
9572|Kimberley Group|36551|6|Mentioned|Table 10|||||||||
9572|Kimberley Group|36885|4|Described|p183|||||||||
9572|Kimberley Group|36898|6|Mentioned|p183|||||||||
9572|Kimberley Group|36902|6|Mentioned|p11|||||||||
9572|Kimberley Group|37462|3|Fully described|p238|||Also described Table 4.III||||||
9572|Kimberley Group|37577|6|Mentioned|p32|||||||||
9572|Kimberley Group|37927|6|Mentioned|p506|||||||||
9572|Kimberley Group|38243|6|Mentioned|p353|||||||||
9572|Kimberley Group|38482|6|Mentioned|Table 1|||||||||
9572|Kimberley Group|38988|6|Mentioned|p14|||See also Fig.4||||||
9572|Kimberley Group|39116|6|Mentioned|p134|||||||||
9572|Kimberley Group|40105|6|Mentioned|p316|||||||||
9572|Kimberley Group|41158|6|Mentioned|p20|||||||||
9572|Kimberley Group|41453|6|Mentioned|p239|||||||||
9572|Kimberley Group|41703|6|Mentioned|p230|||||||||
9572|Kimberley Group|41987|5|Briefly described|Fig.4 P74|||||||||
9572|Kimberley Group|42149|5|Briefly described|Table 1 P709|||||||||
9572|Kimberley Group|42190|6|Mentioned|p269|||||||||
9572|Kimberley Group|42342|6|Mentioned|p23|||||||||
9572|Kimberley Group|42710|5|Briefly described|map legend|Proterozoic||||||||
9572|Kimberley Group|42768|6|Mentioned|Fig.6|||||||||
9572|Kimberley Group|42811|4|Described|p22, Fig.5|||||||||
9572|Kimberley Group|42814|4|Described|p12|||||||||
9572|Kimberley Group|42815|5|Briefly described|map|Proterozoic||||||||
9572|Kimberley Group|43281|5|Briefly described|Map legend||Proterozoic|||||||
9572|Kimberley Group|43561|6|Mentioned|p1438|||||||||
9572|Kimberley Group|43595|5|Briefly described|p443|||||||||
9572|Kimberley Group|43631|6|Mentioned|p10|||Kimberley region||||||
9572|Kimberley Group|43652|6|Mentioned|p385||Paleoproterozoic|||||||07-NOV-08
9572|Kimberley Group|43666|6|Mentioned|p7|||||||||
9572|Kimberley Group|43863|5|Briefly described|map legend|Proterozoic|Proterozoic|||||||
9572|Kimberley Group|44140|5|Briefly described|p293-300|Paleoproterozoic|Paleoproterozoic|Fluvial. Has min age based on 1762 +/-15 Ma Rb-Sr whole rock of intrusive Hart Dolerite (Page, 1976).|>1762 +/- 15 Ma (Rb-Sr).||King Leopold, Warton, Pentecost Sandstones; Carson Volcanics; Elgee Siltstone.|"Subconformably" overlies Speewah Group. Is overlain conformably by Bastion Group and unconformably by Colombo Sandstone. Is intruded by Hart Dolerite.|Contains mature and laterally uniform sandstone and siltstone together with tholeiitic basalt and beds of dolomite.|07-MAR-18
9572|Kimberley Group|44155|6|Mentioned|p236 Fig.3-35, p250, p254 Fig.3-40|Paleoproterozoic|Paleoproterozoic|||||||
9572|Kimberley Group|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes King Leopold Sandstone, Carson Volcanics, Warton Sandstone, Elgee Siltstone and Pentecost Sandstone.Age: >1790Ma. Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|44286|5|Briefly described|Map legend|||||||||
9572|Kimberley Group|44317|14|Not recorded|p.6||Carpentarian|||||||
9572|Kimberley Group|44318|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
9572|Kimberley Group|44324|14|Not recorded|p.7||Carpentarian|Tb.2. (Carpentarian).||||||
9572|Kimberley Group|44325|14|Not recorded|map legend||Carpentarian|Carpentarian.||||||
9572|Kimberley Group|44363|4|Described|p.3,9,11,12,13,16,22|||(Carpentarian) units.||||||
9572|Kimberley Group|44364|14|Not recorded|map legend|||||||||
9572|Kimberley Group|44366|14|Not recorded|p.15, Table 2||Carpentarian|||||||
9572|Kimberley Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
9572|Kimberley Group|44397|14|Not recorded|p.6,9,17,19,Fig4,Tb2||Carpentarian|||||||
9572|Kimberley Group|44694|5|Briefly described|Map Legend||Proterozoic|||||||
9572|Kimberley Group|44867|5|Briefly described|Map Legend||Mesoproterozoic|||||||
9572|Kimberley Group|44868|5|Briefly described|Map Legend||Proterozoic|||||||
9572|Kimberley Group|45038|14|Not recorded|Fig.35|||||||||
9572|Kimberley Group|45047|5|Briefly described|p28|||Carpentarian||||||
9572|Kimberley Group|45077|4|Described|p7|||||||||
9572|Kimberley Group|48927|6|Mentioned|p10|||Overlain unconformably by Kuniandi Gp.||||||
9572|Kimberley Group|48931|3|Fully described|p50|||||||||
9572|Kimberley Group|50009|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Deposited in a broad, semi-enclosed, shallow marine basin. Overlies Speewah Group unconformably and disconformably. Geological Province: Kimberley Basin.||||||07-NOV-08
9572|Kimberley Group|60533|5|Briefly described|p591|Paleoproterozoic|Paleoproterozoic|Age: ca. 1800Ma. Subjected to amphibolite grade metamorphism in southwest.||||||07-NOV-08
9572|Kimberley Group|60714|5|Briefly described|p111, p113.|Orosirian|Orosirian|Kimberley Basin. Max age U-Pb SHRIMP zircon age 1834 +/- 3 Ma from the felsic volcanic racks interbedded in the Valentine Siltstone|1834 +/- 3||Includes King Leopold, Warton and Pentecost Sandstones; Carson Volcanics and Elgee Siltstone.|Unconformably overlies Speeewah Group.||
9572|Kimberley Group|60724|5|Briefly described|p4, p5 Fig. 2|||Intruded by Hart Dolerite. ||||||
9572|Kimberley Group|60844|5|Briefly described|pp15-16. |Late Paleoproterozoic|Late Paleoproterozoic|Of the Kimberley Basin; covers most of the Kimberley Region.|c.1800 - 1790 Ma.||Includes King Leopold Sandstone.|Overlies Speewah Group.||
9572|Kimberley Group|61056|5|Briefly described|p785 Tb. 2|||Intruded by Hart Dolerite in ca. 1800Ma.||||||
9572|Kimberley Group|61571|5|Briefly described|p657 Fig. 4|Paleoproterozoic|Paleoproterozoic|Includes King Leopold Sandstone, Carson Volcanics, Warton Sandstone, Elgee Siltstone and Pentecost Sandstone. Overlain by Mount House Group. mentioned in the context of "post-Kimberley Group folds".||||||07-NOV-08
9572|Kimberley Group|61574|5|Briefly described|p690|Proterozoic|Proterozoic|Includes the Pentecost Sandstone.||||||07-JAN-10
9572|Kimberley Group|61861|6|Mentioned|Fig.2.|||Halls Creek, eastern zone.||||Is intruded by Hart Dolerite. Is unconformably overlain by Bastion Group.||
9572|Kimberley Group|62715|6|Mentioned|p1753|||Intruded by Aries kimberlite. Geological Province: Kimberley Basin.||||||
9572|Kimberley Group|63866|4|Described|p127, p130, p132-p133, p137|Statherian|Orosirian|Western Zone, Halls Creek Orogen. Intruded by the Hart Dolerite. |c. 1800 Ma||Includes the Carson Volcanics.|Unconformably overlies the Moola Bulla Formation, Koongie Park Formation and the McHale Granodiorite. Unconfromably overlain by the Mount Parker Formation and the Bungle Bungle Dolomite.|Sandstone, siltstone and mudstone.|
9572|Kimberley Group|64104|6|Mentioned|p75, p76 fig 10|Paleoproterozoic|Paleoproterozoic|Suggested source of sedimentary clasts in Duerdin Group in Texas/Mabel Downs and Purnululu area.|||Includes Elgee Siltstone.|||
9572|Kimberley Group|64580|6|Mentioned|map legend|||||||||
9572|Kimberley Group|64722|5|Briefly described|Fig. 2 p3-6, p9|Statherian|Orosirian|A sedimentary overlap succession that accumulated across the Kimberley Block and Halls Creek Orogen between 1835 and 1750 Ma.||||||
9572|Kimberley Group|64724|5|Briefly described|p45, Fig.5, p46|Statherian|Statherian|Deposited on the Kimberley Craton ~1800 Ma, either during the waning stages of the Halls Creek Orogeny or the initial stages of the Leichhardt Extension.||||Overlies the Speewah Group.||02-APR-12
9572|Kimberley Group|64748|4|Described|p269 Fig 2, Tb.1, p268, 270, 275, 277-8|Statherian|Orosirian|Includes King Leopold Sandstone, Elgee Sandstone; unconformably underlies Bastion Group in NE; max age 1834+/-3Ma; min age 1790+/-4Ma from Hart Dolerite intrusion; includes red beds used for palaeomag studies; diagenetic xenotime ages ~1704Ma for units in this group; broadly coeval with the Earaheedy Group ||||||
9572|Kimberley Group|66845|6|Mentioned|p536 Fig.2|||||||||
9572|Kimberley Group|66846|6|Mentioned|p549 Fig.2|Statherian|Orosirian|In all zones of the Lamboo Complex.|||||Terriginous clastic rock.|
9572|Kimberley Group|67269|6|Mentioned|p20-21 Fig.19||||||Pentecost Sandstone.|||
9572|Kimberley Group|67484|6|Mentioned|p294|Paleoproterozoic|Paleoproterozoic|||||||
9572|Kimberley Group|67563|5|Briefly described|p120, p120 Fig.1, p125, p129 Tb.2, p131|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.|||Includes King Leopold Sandstone, Carson Volcanics, Warton Sandstone, Elgee Siltstone, and Pentecost Sandstone.|Intruded by the Hart Dolerite. Underlain by the Speewah Group.|Comprises quartz sandstone, siltstone, and mafic volcanic rocks.|20-JAN-17
9572|Kimberley Group|67620|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Appears as Kimberley Basin Group.||||||
9572|Kimberley Group|68078|4|Described|p1, p5-8, p14 figure 10, p17-19, p23-25|Paleoproterozoic|Paleoproterozoic|The six formations of this group form an apparently conformable sequence throughout the Kimberley region. Deposited within a broad, semi-enclosed shallow marine basin. Paleocurrents indicate sediment transport from the north and north west. Maxiumum age for the kimberley group is provided by the date of 1835 Ma for the felsic volcanic unit of the valentine siltstone.|<1835 Ma ||Includes King Leopold Sandstone, Carson Volcanics, Warton Sandstone, Pentecost Sandstone, Elgee Siltstone, Yampi Formation|Unconformably/(disconformably?) overlies Speewah group|Greater than 3km thick.The bulk of this group consists of quartz sandstone, feldspathic sandstone, siltstone, conglomerate and mafic volcanic rocks.|13-SEP-22
9572|Kimberley Group|68244|6|Mentioned|p659,661,664|Late Paleoproterozoic|Late Paleoproterozoic|Kimberley Basin.|||Includes Carson Volcanics and Pentecost Sandstone.|Overlain unconformably by Mount House Group and Kuniandi Group.||
9572|Kimberley Group|68992|5|Briefly described|p498, p498 Fig.1, p499|||Kimberley Basin.|||Includes the Pentecost Sandstone, Elgee Siltstone, Warton Sandstone, Carson Volcanics, and King Leopold Sandstone.|Underlain by the Speewah Group. Intruded by the Hart Dolerite.|Comprises siliciclastic rocks.|
9572|Kimberley Group|69003|6|Mentioned|p5, p18-21|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.||||||
9572|Kimberley Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. The lower Kimberley Group (up to the Carson Volcanics) is older than 1797 +/- 11 Ma, based on the age of the Hart Dolerite, which intrudes it and younger than 1835+/-3 Ma Valentine Siltstone in underlying Speewah Group. Unit relationships from geochron files 182104.1.pdf, 109639.1.pdf. |||Includes Pentecost Sandstone, Elgee Siltstone, Warton Sandstone, Carson Volcanics, King Leopold Sandstone,?and Yampi Formation in 2008.|Unconformably overlies Speewah Group and Lamboo Complex. Intruded by Hart Dolerite.|Quartz sandstone and feldspathic sandstone; siltstone and mudstone; basalt; minor dolostone and conglomerate|21-JUL-15
9572|Kimberley Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|||Includes Pentecost Sandstone, Elgee Siltstone, Warton Sandstone, Carson Volcanics, King Leopold Sandstone||Undivided; quartz sandstone and feldspathic sandstone; siltstone and mudstone, basalt, minor dolostone and conglomerate.|
9572|Kimberley Group|69435|6|Mentioned|p20:1|||Possible correlative of the Fitzmaurice Group.||||||12-JUL-16
9572|Kimberley Group|69585|4|Described|p1-5, p18-32|Statherian|Orosirian|Fluvial and shallow-marine succession, deposited during and immediately after the 1835-1810 Ma Halls Creek Orogeny. Typically ~3km thick. The constituent units are thought to be conformable, except perhaps between Carson Volcanics (upper limit of Hart Dolerite intrusions) and Warton Sandstone. Contains significant Neoarchean crust-sourced sediments, unlike Speewah Group: significance discussed. Deformed during Yampi and King Leopold Orogenies.|1835-1797 Ma (lower part: Page and Sun, 1994).||King Leopold, Warton, Pentecost Sandstones; Elgee Siltstone; Carson Volcanics; Yampi Formation.|Unconformably overlies Speewah Group. Is intruded by Hart Dolerite.|Dominantly quartz and feldspathic sandstone, siltstone, claystone, conglomerate, mafic volcanic rocks, and rare dolostone.|
9572|Kimberley Group|69597|5|Briefly described|p3, p5 fig 2b, p55|Paleoproterozoic|Paleoproterozoic|4km thick. Kimberley Basin. |c. 1800 Ma|||Overlies the Speewah Group. Intruded by the Hart Dolerite. Unconformably overlain by the Carr Boyd Group.|Siliciclastic sedimentary rocks and mafic volcanic rocks.|
9572|Kimberley Group|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Kimberley Basin. Events: King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1; King Leopold Orogeny D1/M1; Yampi Orogeny D1/M1.  See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 250k_geologyp_lut.csv, 500k_interpgeop_lut.csv, 250k_interpgeop_lut.csv and geochron files.|1835-1740 Ma (Inferred)||Includes Carson Volcanics, King Leopold Sandstone, Pentecost Sandstone, Warton Sandstone, Yampi Formation.|Underlain unconformably by Speewah Group.|Quartz sandstone and feldspathic sandstone; siltstone and mudstone; basalt; minor dolostone and conglomerate|
9572|Kimberley Group|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, Kimberley Craton.|||Includes King Leopold, Warton, Pentecost Sandstones; Carson Volcanics; Elgee Siltstone.||Sandstones, siltstones, mudstones, dolostone; minor conglomerate.|
9572|Kimberley Group|70126|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin; North Australian Craton.|||King Leopold, Warton, Pentecost Sandstones; Carson Volcanics; Elgee Siltstone.||Sandstones, siltstones, chert and basalt.|
9572|Kimberley Group|70131|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||Lower Kimberley Group, Upper Kimberley Group.|||
9572|Kimberley Group|70154|4|Described|100k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 2_5m_geologyp98_lut.csv, 100k_interpgeop_lut.csv.|1740-1835 Ma||Carson Volcanics, Elgee Siltstone, King Leopold Sandstone, Pentecost Sandstone, Warton Sandstone||Quartz sandstone and feldspathic sandstone; siltstone and mudstone; basalt; minor dolostone and conglomerate.|
9572|Kimberley Group|70217|5|Briefly described|p3, p5 fig 2b, p55|Paleoproterozoic|Paleoproterozoic|4km thick. Kimberley Basin. |c. 1800 Ma|||Overlies the Speewah Group. Intruded by the Hart Dolerite. Unconformably overlain by the Carr Boyd Group.|Siliciclastic sedimentary rocks and mafic volcanic rocks.|
9572|Kimberley Group|70731|4|Described|p268,270,272,274,276,278|Stathetian|Stathetian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Provenance from the N and NW basin margins dominated by Neoarchean 2525-2480 Ma detrital zircons (Hollis et al., 2014). Difference in provenance and regional unconformity with underlying Speewah Group reflect major change in basin-forming processes (extensional collapse of lithsphere following Halls Creek Orogeny; Hollis et al., 2014). Neoarchean basement also exposed during Kimberley Group deposition (Hollis et al., 2014).|||Includes Pentecost Sandstone, Elgee Siltstone, Warton Sandstone and King Leopold Sandstone.|Overlain by Bastion Group.||
9572|Kimberley Group|70760|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||Lower Kimberley Group (King Leopold Sandstone, Carson Volcanics); Upper Kimberley Group (Warton Sandstone, Elgee Siltstone, Pentecost Sandstone).|Is intruded by Hart Dolerite.|Sandstone, siltstone, mudstone, basalt and basaltic volcaniclastic rocks.|
9572|Kimberley Group|70761|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||Lower Kimberley Group (King Leopold Sandstone, Carson Volcanics); Upper Kimberley Group (Warton Sandstone, Elgee Siltstone, Pentecost Sandstone).|Is intruded by Hart Dolerite.|Sandstone, siltstone, mudstone, basalt and basaltic volcaniclastic rocks.|
9572|Kimberley Group|70812|5|Briefly described|p3, p5-p6|||Western Zone of the Halls Creek Orogen, Lamboo Province.|||Includes the Lower Kimberley Group and Upper Kimberley Group.|Unconforambly overlies the Speewah Group. Intruded by the Hart Dolerite.||
9572|Kimberley Group|70826|6|Mentioned|p2, p5 tbl 2, p9, p10|Paleoproterozoic|Paleoproterozoic|Kimberley Basin.|||upper Kimberley Group, lower Kimberley Group|Is intruded by the Hart Dolerite.||
9572|Kimberley Group|70851|5|Briefly described|p2, p6, p24|||See also Kimberley Group, Lower and Kimberley Group, Upper. Geophysical characteristics are discussed.|||||Sedimentary rocks.|29-MAR-23
9572|Kimberley Group|71113|5|Briefly described|p101|Paleoproterozoic|Paleoproterozoic|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Of the Kimberley Basin. Siliciclastic sedimentary and mafic volcanic rocks in the post-collisional extensional setting.|c. 1800 Ma|||Underlain unconformably by Speewah Group.||
9572|Kimberley Group|71140|6|Mentioned|p101|Orosirian|Orosirian|Post-(Halls Creek Orogeny)-collisional Kimberley Basin.|c.1800 Ma.|||Unconformably overlies the Speewah Group.|A succession of siliciclastic sedimentary and mafic volcanic rocks.|
9572|Kimberley Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological provice: Halls Creek Orogen; King Leopold Orogen. Of Kimberley Basin. Sequence of Paleoproterozoic rocks. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 1m_interpgeop_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv and geochron files.|1835-1740 Ma (inferred)||Includes Elgee Siltstone, Carson Volcanics, King Leopold Sandstone, Pentecost Sandstone, Warton Sandstone, Yampi Formation.|Intruded by Wotjulum Porphyry. Underlain unconformably by Speewah Group.|Quartz sandstone, minor fine- to medium-grained feldspathic sandstone; micaceous and glauconitic sandstone, shale pellet conglomerate; siltstone, quartz basalt, argillaceous quartz sandstone|
9572|Kimberley Group|71281|4|Described|p419, p421, p423, p429|Paleoproterozoic|Paleoproterozoic|Kimberley Basin. c.4km thick succession of marine deposits. Has an outcrop area of 400 x 400 km. Deposition post-dates the Halls Creek Orogeny. Age range from stratigraphic relationships.|c.1835 Ma - c. 1740 Ma.||King Leopold, Warton, Pentecost Sandstones; Elgee Siltstone; Carson Volcanics.|Unconformably overlies Speewah Group. Is intruded by Hart Dolerite.|Predominantly marine siliciclastic rocks with shallow-water depositional structures.|07-DEC-18
9572|Kimberley Group|71397|5|Briefly described|p5-6|Statherian|Orosirian|Geological province: Western Zone, Lamboo Province, Halls Creek Orogen. Mylonites on the margins of Kimberley Group likely associated with c. 1000-800 Ma Yampi Orogeny (Tyler and Griffin, 1990; Tyler et al., 1995).||||Intruded by Wotjulum Porphyry.||
9572|Kimberley Group|71811|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Kimberley Basin, North Australian Craton.|||King Leopold, Warton, Pentecost Sandstones; Elgee Siltstone; Carson Volcanics.|||
9572|Kimberley Group|72034|6|Mentioned|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Mentioned as parent unit. Age assumed from constituents. No other data. Informally subdivided into Kimberley Group, lower; Kimberley Group, upper.|||Includes lower part: Carson Volcanics, King Leopold Sandstone; upper part: Yampi Formation, Pentecost Sandstone, Elgee Siltstone, Warton Sandstone.|||
9572|Kimberley Group|72437|6|Mentioned|p12-13||||||Includes the basal Carson Volcanics and the Elgee Siltstone.|||
9572|Kimberley Group|72490|5|Briefly described|p2-5, p11|||Intruded by Hart Dolerite up to the basal part of the Carson Volcanics.|||Pentecost Sandstone, Elgee Siltstone, Warton Sandstone, King Leopold Sandstone, Carson Volcanics, and Hart Dolerite[?]|Intruded by Hart Dolerite.|Greenschist facies metamorphics.|
9612|Kings Park Formation|12759|1|Redefined|p42-3; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Eocene|Paleocene|Redefined Quilty (1974) and this study. Type section in Kings Park No.2 bore, (AMG Zone 50, 390556m E, 6461738m N) between 23-492 m depth. Max thickness is 530 m. Forms 2 minor confined aquifers.|||Includes Mullaloo Sandstone, and Como Sandstone (this study), Members.||Grey, calcareous, glauconitic siltstone and shale of shallow marine to estuarine origin.|12-MAY-14
9612|Kings Park Formation|14227|5|Briefly described|Enclos. 2|Eocene|Palaeocene|Presented as Kings Park Fm.||||||07-FEB-11
9612|Kings Park Formation|22769|5|Briefly described|p755,758-60||Paleocene|Deposits apparently fill an old, deeply incised river valley system.  Geological Province: Perth Basin.||||||17-JAN-06
9612|Kings Park Formation|23880|5|Briefly described|p42|Early Eocene|Late Paleocene|||||||
9612|Kings Park Formation|24058|5|Briefly described|p116|Tertiary|Tertiary|Geological Basin: Perth Basin.||||||
9612|Kings Park Formation|24455|5|Briefly described|p327|||Composed of dark glauconitic shales, siltstones and sandstones.  Max. thickness: 500m. Geological Province: Perth Basin. See also p321 Fig. 1.||||||22-MAR-05
9612|Kings Park Formation|29382|6|Mentioned|Table 10|||||||||
9612|Kings Park Formation|29693|6|Mentioned|Fig.7|||||||||
9612|Kings Park Formation|31051|6|Mentioned|p83|||||||||
9612|Kings Park Formation|31054|6|Mentioned|p45|||||||||
9612|Kings Park Formation|31562|5|Briefly described|p13|||Depositional environment||||||
9612|Kings Park Formation|31568|6|Mentioned|p19|||Palaeocene - Eocene Fig. 2||||||
9612|Kings Park Formation|32117|6|Mentioned|p84|||||||||
9612|Kings Park Formation|32714|6|Mentioned|Fig.2|||||||||
9612|Kings Park Formation|32748|4|Described|p20|||See also P27. Map. P19||||||
9612|Kings Park Formation|32750|3|Fully described|p307|||Refers Wells (1943), Glaessner (1956) & McGowran (1966). See P304||||||
9612|Kings Park Formation|32752|6|Mentioned|Fig.3|||||||||
9612|Kings Park Formation|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
9612|Kings Park Formation|33386|6|Mentioned|Fig.7|||||||||
9612|Kings Park Formation|33801|6|Mentioned|p51|||||||||
9612|Kings Park Formation|34951|6|Mentioned|p109|||||||||
9612|Kings Park Formation|35093|6|Mentioned|Fig.13|||||||||
9612|Kings Park Formation|35100|6|Mentioned|p165|||||||||
9612|Kings Park Formation|35282|6|Mentioned|Fig.6|||||||||
9612|Kings Park Formation|35970|6|Mentioned|p76|||See also Table 12.||||||
9612|Kings Park Formation|36257|6|Mentioned|Table 2.1|||||||||
9612|Kings Park Formation|36293|2|Defined|p197|Eocene|Paleocene|Eocene to Palaeocene||||||
9612|Kings Park Formation|36305|6|Mentioned|p354|||||||||
9612|Kings Park Formation|37062|6|Mentioned|p182|||||||||
9612|Kings Park Formation|38221|6|Mentioned|p354|||||||||
9612|Kings Park Formation|39156|6|Mentioned|Table 4|||||||||
9612|Kings Park Formation|39211|6|Mentioned|Fig.41|||||||||
9612|Kings Park Formation|39923|6|Mentioned|p353|||||||||
9612|Kings Park Formation|40395|6|Mentioned|p332|||||||||
9612|Kings Park Formation|40992|6|Mentioned|Fig.5|||||||||
9612|Kings Park Formation|41751|6|Mentioned|p7|||||||||
9612|Kings Park Formation|41912|6|Mentioned|p27|||||||||
9612|Kings Park Formation|41989|6|Mentioned|Fig.3 P110|||||||||
9612|Kings Park Formation|42687|6|Mentioned|map legend|Tertiary||||||||
9612|Kings Park Formation|43700|6|Mentioned|Fig.2,p21|Eocene|Paleocene|||||||
9612|Kings Park Formation|44144|4|Described|p503 Tb.4-21, p509 Fig.4-145, p518|Early Eocene|Late Paleocene|Type Section: Kings Park 2 bore; 31o58'30''S 115o50'30''E; 23-361m.  532m thick shallow marine deposits.|||Includes Mullaloo Sandstone Member.|Overlies Coolyena,r Warnbro Groups disconformably; Parmelia, Yarragadee Formations unconformably. Overlain by Stark Bay, Challenger Formations disconformably, and Guildford Formation unconformably.|Grey, often glauconitic, siltstone, shale and minor poorly sorted sandstone at top.|
9612|Kings Park Formation|61155|5|Briefly described|p3, p15|Early Eocene|Late Paleocene|Glauconitic mudstone, sandstone and limestone. Overlain by and interfingers with Mullaloo Sandstone. Age: 60-56Ma. Max. thickness: 500m. Geological Province: Perth Basin. ||||||
9612|Kings Park Formation|63745|5|Briefly described|p64 Fig. 3|Eocene|Paleocene|Unconformable below Perth Formation.||||||07-FEB-11
9612|Kings Park Formation|65194|5|Briefly described|p122|Eocene|Eocene|||||||
9612|Kings Park Formation|67135|6|Mentioned|p33 Fig.42.|||A confining bed for aquifers in the Perth Basin.||||||
9612|Kings Park Formation|67925|6|Mentioned|Ch4 p8 fig 2|||||||Unconformably overlies the Coolyena Group. Unconformably overlain by the Stark Bay Formation.||
9612|Kings Park Formation|68254|6|Mentioned|p1036 Fig.2, p1040 Tb.3, p1046 Tb.4|Paleogene|Cretaceous||||Includes Mullaloo Sandstone and Como Sandstone.|||
9612|Kings Park Formation|68811|5|Briefly described|p92 fig 52, p180 tbl 39|Tertiary|Tertiary||||Includes the Mullaloo and Como Sandstone Members.|Overlies the Lancelin Formation.|Siltstone, shale and minor sandstone.|
9612|Kings Park Formation|70099|5|Briefly described|Fig.4; p6|Eocene|Paleocene|Selandian-Thanetian Stages. Southern Perth Basin. Correlated to deep marine, carbonate-dominated sedimentation of the Mentelle 10 Supersequence.||||||
9612|Kings Park Formation|70128|5|Briefly described|p449|Paleogene|Paleogene|Central Perth Basin.||||Unconformably overlies Coolyena Group. Is overlain unconformably by Ascot Formation and Kwinana Group.||
9623|Kinmore Group|5952|5|Briefly described|p221 Fig. 15|Permian|Permian|Includes Hyland Bay Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
9623|Kinmore Group|13194|4|Described|p387 Tb. 4-16|Triassic|Permian|460-2000m thick.|||Mount Goodwin Formation|Overlies Kulshill Group (conformably).||
9623|Kinmore Group|13222|6|Mentioned|p229 Fig.2.|||Gorter (1998) omits Hyland Bay Formation and lists several Formations (not Members).|||Includes Fossil Head, Mount Goodwin and Hyland Bay Formations.|||
9623|Kinmore Group|13224|6|Mentioned|p485 fig 3|Scythian|Kazanian|||||||
9623|Kinmore Group|13242|5|Briefly described|p214 Fig. 2|Late Permian|Late Permian|Defined by Mory (1988, 1991) who included Fossil Head and Mount Goddwin Formations - excluded in this paper. Geological Province: Bonaparte Basin.||||||07-FEB-11
9623|Kinmore Group|13354|6|Mentioned|p375 Fig.6.|Permian|Late Carboniferous|Comprises, in ascending order, Kulshill Group, Fossil Head Formation and Hyland Bay Formation.||94||||28-OCT-14
9623|Kinmore Group|22663|5|Briefly described|AC97 1-4 Fig.4||Permian|||||||01-MAR-10
9623|Kinmore Group|24569|5|Briefly described|p248 Fig. 3|Triassic|Permian|Includes the Fossil Head, Hyland Bay and Mount Goodwin Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
9623|Kinmore Group|41459|6|Mentioned|p283|||Reserved as Kinmore Member. See also Fig.2||||||
9623|Kinmore Group|41532|3|Fully described|p301|||||||||
9623|Kinmore Group|41689|6|Mentioned|Table 1|||||||||
9623|Kinmore Group|41731|6|Mentioned|Fig.3|||||||||
9623|Kinmore Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
9623|Kinmore Group|42055|4|Described|Fig.1 P52|||||||||
9623|Kinmore Group|42056|5|Briefly described|Fig.6 P95|||||||||
9623|Kinmore Group|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
9623|Kinmore Group|42075|5|Briefly described|Fig.4 P245|||||||||
9623|Kinmore Group|42442|3|Fully described|p17|Anisian|Artinskian|Equivalent to 'Port Keats Group' of Noakes 1949. Variation on Kinmore Group, WA.||||||03-AUG-06
9623|Kinmore Group|43661|6|Mentioned|Fig.3|||||||||
9623|Kinmore Group|43699|6|Mentioned|Fig.6,p10|Middle Triassic|Early Triassic|||||||
9623|Kinmore Group|43707|5|Briefly described|Fig.3,p4||Permian|||||||
9623|Kinmore Group|43739|6|Mentioned|p10||Permian|||||||
9623|Kinmore Group|49637|5|Briefly described|Fig.3|Early Triassic|Late Permian|Includes the Fossil Head, Hyland Bay and Mount Goodwin Formations. Geological Province: Petrel Sub-basin.||||||07-FEB-11
9623|Kinmore Group|60634|6|Mentioned|p1168 Fig.3. |Permian|Permian||||Includes Hyland Bay Formation.|Is overlain by Sahul Group.||
9623|Kinmore Group|62837|5|Briefly described|Stratigraphic columns|Early Triassic|Early Permian|Includes Fossil Head, Hyland Bay and Mount Goodwin Formations.  Age: ~287-~242 Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
9623|Kinmore Group|64698|4|Described|lithinterp table|Kungurian|Asselian|Age ~275-298Ma (Early Permian). Bonaparte Basin. Max. thickness 1800m. Succession of basal conglomerate followed by siltstone, silty sandstone, limestone and minor diamictite.||||||07-JAN-09
9623|Kinmore Group|67354|6|Mentioned|p73. |||Includes Permian and early Triassic strata that were formerly part of the Port Keats Group.||||||
9623|Kinmore Group|67370|5|Briefly described|p313 Fig.2, p332. |Triassic|Permian|Revised. Mount Goodwin Formation is raised to Subgroup rank.|||Includes the lower Fossil Head Formation, the middle Hyland Bay Subgroup and the upper Mount Goodwin Subgroup.|Is overlain by Troughton Group.||
9623|Kinmore Group|69297|6|Mentioned|p305, p322|Olenekian|Guadalupian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||||Overlain by the Sahul Group.||
9623|Kinmore Group|69452|5|Briefly described|p36:4-5, 8, 15, 18-21|Middle Triassic|Permian|Mory (1991); redefined in Gorter (1998) and Gorter et al. (2009). Equivalent to Port Keats Group of Noakes (1949). Discontinuous outcrop; extensive in the subsurface.|||Mount Goodwin, Hyland Bay Subgroups; Fossil Head Formation.|Unconformably overlies Kulshill Group. Is overlain unconformably by Troughton Group.||12-JUL-16
9623|Kinmore Group|69454|5|Briefly described|p38:4|Olenekian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.|||Hyland Bay, Mount Goodwin Subgroups.|Overlies Kulshill Group. Is overlain by Troughton Group.||12-JUL-16
9623|Kinmore Group|69653|5|Briefly described|p10, 14-15|Triassic|Permian|Petrel Sub-basin. Tidal shelf environment, succeeded by shallow-marine transgressive sediments. Forms an extensive regional seal.|||Hyland Bay Sub-group; Mount Goodwin Sub-group; Fossil Head Formation.|Overlies Kulshill Group. Is overlain by Troughton Group.|Thick transgressive sequences of marine mudstones and siltstones, succeeded by shallow-marine sandstones, mudstones and carbonates, topped by marine shales and siltstones.|
9623|Kinmore Group|69673|6|Mentioned|p166 fig 136, p168 fig 138, p173|Triassic|Permian ||||Includes Fossil Head Formation, Hyland Bay Subgroup, Mount Goodwin Subgroup|Unconformably overlies Kulshill Group||
9623|Kinmore Group|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3|Olenekian|Artinskian|See also Regional geology: Figs.6-8, p8. Sahul: p2. Vulcan: Fig.2, p2. Source rock in Sahul Syncline.|||Mount Goodwin, Hyland Bay Subgroups; Fossil Head Formation.|Overlies Kulshill Group. Is overlain by Troughton Group.||12-JUL-16
9623|Kinmore Group|70064|5|Briefly described|Regional Fig. 6. Central Fig.2; p2|Anisian|Sakmarian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins and Prudhoe Terrace, Browse Basin. Equivalent units in Central Caswell Sub-basin are potential reservoirs.|||Hyland Bay, Mount Goodwin Sub-groups.|Overlies Kulshill Group. Is overlain by Sahul Group.||12-JUL-16
9623|Kinmore Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone|
9630|Kintore Tonalite|42697|5|Briefly described|map legend|Archean||Not related to Kintore Granite, Qld. Invalidates the reservation of Kintore Dam Formation, WA.||||||07-NOV-08
9630|Kintore Tonalite|42892|5|Briefly described|p46|||||||||
9630|Kintore Tonalite|43102|5|Briefly described|Fig.4|||||||||
9630|Kintore Tonalite|43232|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
9630|Kintore Tonalite|60076|6|Mentioned|p46 App. 1|||[Agtkn]  Medium-grained biotite tonalite.||||||13-APR-05
9630|Kintore Tonalite|65204|6|Mentioned|p19 Tbl.4.|Neoarchean||Medium grains; equigranular.||||||
9630|Kintore Tonalite|65264|5|Briefly described|p47 Appdx. 1|Archean|Archean|Medium-grained biotite monzogranite.||||||07-FEB-11
9630|Kintore Tonalite|69152|4|Described|GEOL_LUT_CSV files + geochron files|Neoarchean|Neoarchean|Yilgarn Craton|||||Medium-grained biotite tonalite.|06-AUG-15
9630|Kintore Tonalite|70153|5|Briefly described|100k_interpgeop_lut.csv|Neoarchean|Mesoarchean||3010 - 2600 Ma (inferred).||||Medium-grained biotite tonalite; metamorphosed.|
9630|Kintore Tonalite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||tonalite|
9630|Kintore Tonalite|71270|4|Described|GEOL_LUT_CSV files|Neoarchean|Mesoarchean|Geological province: Yilgarn Craton, West Australian Craton. Events: Yilgarn Craton granite magmatism (3010 - 2600 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp10_lut.csv, 1m_geologyp12_lut.csv.|3010-2600 Ma (inferred)||||Medium-grained biotite tonalite; metamorphosed|
9637|Kirkby Range Member|22741|5|Briefly described|P29, Table3 P12||Late Permian|||||||
9637|Kirkby Range Member|22767|5|Briefly described|Table3 p14, P22||Late Permian|||||||04-NOV-15
9637|Kirkby Range Member|22776|4|Described|Table.3|Late Permian|Late Permian|Hardman Fm. Liveringa Group.||||||
9637|Kirkby Range Member|30342|6|Mentioned|Table 20|||||||||
9637|Kirkby Range Member|33518|4|Described|Table 1|||||||||
9637|Kirkby Range Member|33519|6|Mentioned|Map legend|Permian|Permian|||||||
9637|Kirkby Range Member|33962|2|Defined|p50|Permian|Permian|||||||
9637|Kirkby Range Member|36224|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Hardman Formation.  Mudstone, fine sandstone, calcareous, lamintaed to thin bedded, ripple marked; minor conglomerate lenses; fossiliferous.||||||04-NOV-15
9637|Kirkby Range Member|36225|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
9637|Kirkby Range Member|36634|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
9637|Kirkby Range Member|41158|6|Mentioned|p162|||||||||
9637|Kirkby Range Member|41540|5|Briefly described|p21|||||||||
9637|Kirkby Range Member|41688|6|Mentioned|p10|||||||||
9637|Kirkby Range Member|42654|6|Mentioned|p3|||||||||
9637|Kirkby Range Member|42994|6|Mentioned|p47|||of Hardman Formation||||||
9637|Kirkby Range Member|45153|6|Mentioned|App.4-73|||See also App.4-77||||||
9637|Kirkby Range Member|45158|4|Described|p18|||||||||
9637|Kirkby Range Member|49644|5|Briefly described|Table|||||||||
9637|Kirkby Range Member|66949|4|Described|p4 Fig.2, p25, p56 Appx.3|Wuchiapingian|Wuchiapingian|Type section detailed. Up to 300m thick (p25 says 75m); regressive marine deposits. Age from macrofauna. Biostratigraphic zonation. Mis-spelt as Kirby Range Mbr in Fig.2.||Basal unit in Hardman Formation.||Overlies Lightjack Formation and Condren Sandstone. Is overlain by Hicks Range Sandstone Member.|Sandstone, lesser sandy siltstone; minor calcareous sandstone.|04-NOV-15
9637|Kirkby Range Member|71623|5|Briefly described|p343, p345 fig 5||Wuchiapingian|Canning Basin. Marine.||Of Hardman Formation.||Overlain by the Hicks Range Member.|Limestone|08-MAY-19
9646|Kirup Conglomerate|23880|5|Briefly described|p42|Eocene|Eocene|Geological Province: Yilgarn Craton.||||||
9646|Kirup Conglomerate|30146|6|Mentioned|p314|||Refs Finkl(71),Taylor(71). Correlated to seds in Darling Plateau.||||||
9646|Kirup Conglomerate|32341|5|Briefly described|p17|||Refers Hobson & Matheson (1949)||||||
9646|Kirup Conglomerate|33801|6|Mentioned|p52|||||||||
9646|Kirup Conglomerate|37340|6|Mentioned|p169|||||||||
9646|Kirup Conglomerate|37341|2|Defined|p245|Permian|Permian|Prob. Permian||||||
9646|Kirup Conglomerate|37350|6|Mentioned|Fig.1|||||||||
9646|Kirup Conglomerate|37633|6|Mentioned|p69|||||||||
9646|Kirup Conglomerate|39834|6|Mentioned|p290|||||||||
9646|Kirup Conglomerate|40358|6|Mentioned|p25|||||||||
9646|Kirup Conglomerate|40359|5|Briefly described|p25|||||||||
9646|Kirup Conglomerate|42280|6|Mentioned|p53|||||||||
9677|Knobby Sandstone|7433|5|Briefly described|p25 Fig.2, p53.|Late Devonian|Late Devonian|Billiluna Shelf, Canning Basin. Coarse fluvial clastics. Radiometric anomalies present warrant investigation for possible uranium deposits.|||||Coarse quartzose clastics.|
9677|Knobby Sandstone|22764|6|Mentioned|p13|||May correlate with Undivided Middle Devonian to Early Carboniferous rocks||||||01-FEB-10
9677|Knobby Sandstone|29813|6|Mentioned|p7|||||||||
9677|Knobby Sandstone|29818|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9677|Knobby Sandstone|33962|2|Defined|p50|Devonian|Devonian|||||||
9677|Knobby Sandstone|35205|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9677|Knobby Sandstone|38878|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
9677|Knobby Sandstone|40866|6|Mentioned|p179|||||||||
9677|Knobby Sandstone|41730|6|Mentioned|p481|||||||||
9677|Knobby Sandstone|42030|6|Mentioned|p748|||||||||
9677|Knobby Sandstone|43173|6|Mentioned|54||Late Devonian|||||||
9677|Knobby Sandstone|43666|6|Mentioned|p17|||||||||
9677|Knobby Sandstone|43818|6|Mentioned|Fig.2.p39|Early Carboniferous|Middle Devonian|||||||
9677|Knobby Sandstone|44143|4|Described|p.439 Table 4-19, p442|Devonian|Devonian|Up to 1000m thick; sandstone, siltstone and conglomerate; fluvial. Type section in Knobby Hills (BILLILUNA: 19deg 24' 24" S, 127deg 45' 44" E). Plant fossils and placoderm fish.||||||23-NOV-17
9677|Knobby Sandstone|45140|5|Briefly described|p65-67|Devonian|Devonian|NE Canning Basin. Fluvial deposits, containing plant and fish fossils. Similar lithology to Pedestal Beds.||||Unconformably overlies Baines and Carranya Beds, and Redcliff Pound Group. Is overlain unconformably by the Grant Formation.|Cross-bedded, medium- to coarse-grained quartzose sandstone and minor amounts of conglomerate and siltstone.|
9677|Knobby Sandstone|45153|2|Defined|App.3-41|Late Devonian|Late Devonian|||||||
9677|Knobby Sandstone|45158|3|Fully described|p26|||||||||
9677|Knobby Sandstone|46864|6|Mentioned|p40|||||||||
9677|Knobby Sandstone|46899|6|Mentioned|p8|||Upper Devonian. Thermal conductivity & geothermal gradient.||||||
9677|Knobby Sandstone|64580|4|Described|map legend|Late Devonian|Middle Devonian|Sandstone, siltstone, conglomerate.||||||09-DEC-08
9677|Knobby Sandstone|64643|5|Briefly described|p3 Fig. 2|Late Devonian|Upper Devonian|||||||10-FEB-20
9677|Knobby Sandstone|65074|6|Mentioned|p360|||Of NE Canning Basin. Appears as Knobby Hills Sandstone.||||Probably correlates with Pedestal beds (Birrindudu Basin).||
9677|Knobby Sandstone|65301|5|Briefly described|p5 Fig. 4|Late Devonian|Late Devonian|Geological province: Canning Basin.||||||
9677|Knobby Sandstone|65449|6|Mentioned|p6|Late Devonian|Late Devonian|||||||
9677|Knobby Sandstone|68007|6|Mentioned|p4|Late Devonian|Late Devonian|Canning Basin.||||||25-FEB-20
9677|Knobby Sandstone|68298|5|Briefly described|p234|Famennian|Famennian|Fragmentary assemblage includes Bothriolepis and an asterolepid, probably Remogolepis, presumed to be of Famennian age (Young, 1987a).||||||
9677|Knobby Sandstone|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Late Devonian|Middle Devonian|Canning Basin. See also 500k_geologyp08_lut.csv.|||||Sandstone, siltstone, conglomerate|
9677|Knobby Sandstone|68902|6|Mentioned|p9 fig 5|Carboniferous|Carboniferous|Appears as ?Knobby Sandstone, together with Clanmeyer/Luluigui Fms.||||||
9677|Knobby Sandstone|69099|5|Briefly described|500k_geologyp08_lut.csv|Late Devonian|Middle Devonian||||||Sandstone, siltstone, conglomerate.|31-JUL-15
9677|Knobby Sandstone|69165|4|Described|500k_geologyp08_lut.csv|Devonian|Devonian||||||Sandstone, Siltstone and conglomerate|
9677|Knobby Sandstone|69312|6|Mentioned|p19|Devonian|Devonian|Canning Basin. ||||Overlies the Nullara Formation. Overlain by the Clanmeyer Siltstone.|Sandstone.|
9677|Knobby Sandstone|69587|5|Briefly described|GEOL_LUT_CSV files|Upper Devonian|Middle Devonian|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|393.3-358.9 Ma (inferred)||||Sandstone, siltstone, conglomerate|
9677|Knobby Sandstone|70129|5|Briefly described|Map legend|Devonian|Devonian|Canning Basin.|||||Sandstone, siltstone and conglomerate.|
9677|Knobby Sandstone|70142|5|Briefly described|Map legend.|||Canning Basin.||||||
9677|Knobby Sandstone|70154|5|Briefly described|500k_interpgeop14_lut.csv|Devonian|Devonian ||359-393 Ma||||Sandstone, siltstone and conglomerate.|
9677|Knobby Sandstone|70774|5|Briefly described|p4|Mississippian|Late Devonian|Canning Basin.||||Overlain by the Fairfield Group.||10-FEB-20
9677|Knobby Sandstone|71267|4|Described|GEOL_LUT_CSV files|Late Devonian|Late Devonian|Of Canning Basin. Events: Point Moody Extension (300-242 Ma); Red Bluffs Extension (372.2-360 Ma); Van Emmerick Extension (382.7-372.2 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|382.7-358.9 Ma (inferred)||||Fluvial fossiliferous medium to coarse grained cross-bedded quartz sandstone with abundant mudstone pellets in places; minor interbedded siltstone and pebble to boulder conglomerate|
9677|Knobby Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Late Devonian|Late Devonian|Canning Basin.|||||Sandstone, siltstone, and conglomerate.|
9696|Kockatea Shale|12729|6|Mentioned|p.15, 28||Early Triassic|Perth Basin. Outcrops in coastal cliffs at Shell House, south of Kalbarri.||||Conformably overlies Wittecarra Sandstone.||
9696|Kockatea Shale|12731|6|Mentioned|p596.|Triassic|Triassic|Long migration of hydrocarbons sourced from this unit from the Edel Terrace is possible in southern Gascoyne Platform.||||||
9696|Kockatea Shale|12758|5|Briefly described|p8 Fig. 9|Early Triassic|Early Triassic|Transitionally overlain by Woodada Fm; unconformably underlain by Wagina Sandstone.  max. thickness: 1100m.  Unit is the seal for the Dingara gas and oilfield.  Correlates with Sabina Sandstone (Southern Perth Basin).  Geol.Prov: Northern Perth Basin.||||||
9696|Kockatea Shale|13242|6|Mentioned|p225|Early Triassic|Early Triassic|Contemporaneous with deposition of Lower Mount Goodwin Formation in the Bonaparte Basin. Geological Province: Perth Basin.||||||07-FEB-11
9696|Kockatea Shale|14227|5|Briefly described|p6, p7, p10|Early Triassic|Early Triassic|Includes Wittecarra Sandstone Member. Geological Province: Perth Basin. See also Enclosure 2.||||||07-FEB-11
9696|Kockatea Shale|14228|5|Briefly described|p5 fig 2, p8, p16-21|Triassic|Triassic|Extends to southern Gascoyne Platform. Major oil-source rock in Perth Basin. Seals the oil of Tumblagooda Sandstone.||||Conformably overlies Wittecarra Sandstone. Overlain by Woodada Formation.||
9696|Kockatea Shale|22814|5|Briefly described|fig2|Triassic|Triassic|||||||
9696|Kockatea Shale|23172|4|Described|Map Legend|Triassic|Triassic|||||||
9696|Kockatea Shale|23279|4|Described|p16,20-2||Scythian|||||||
9696|Kockatea Shale|23520|5|Briefly described|p6 Fig. 4|Early Triassic|Early Triassic|Forms a seal over the Wittecarra Sandstone. Max. thickness: 250m. Geological Province: Abrolhos Sub-basin. See also p9.||||||22-JUL-09
9696|Kockatea Shale|23572|4|Described|p11|Triassic|Triassic|Geological Province: Carnarvon Basin. Underlying Unit: Tumblagooda Sandstone.||||||
9696|Kockatea Shale|23578|5|Briefly described|p7|Early Triassic|Early Triassic|||||||
9696|Kockatea Shale|23579|5|Briefly described|Map Legend|||||||||
9696|Kockatea Shale|23726|5|Briefly described|p15|||Underlying unit Wittecarra Sandstone. Geological Province: Carnarvon Basin.||||||
9696|Kockatea Shale|23815|4|Described|p290|Early Cretaceous|Early Cretaceous|Geological Province: Carnarvon Basin. Max. thickness 15 m. Underlying unit: Wittecarra Sandstone (conformable). Overlyong unit: Birdrong Sandstone (disconformable).||||||13-DEC-07
9696|Kockatea Shale|23816|4|Described|p237|Scythian|Scythian|Geological Province: Perth Basin. Overlying unit: Woodada Formation (conformable). Max. thickness: 300 m.||||||
9696|Kockatea Shale|24058|5|Briefly described|p111|Early Triassic|Early Triassic|Geological Basin: Perth Basin.||||||
9696|Kockatea Shale|24160|6|Mentioned|p94||Triassic|Also mis-spelt as Kokatea on the same page.||||||
9696|Kockatea Shale|24351|5|Briefly described|Plate 3, Plate 4 (in pocket)|Middle Triassic|Early Triassic|Geological Province: Gascoyne Platform/Sub-basin. Log Wittecarra-1.||||||13-DEC-07
9696|Kockatea Shale|24390|5|Briefly described|p14, p15 Fig. 8|Triassic|Triassic|Geological Province: Perth Basin.||||||
9696|Kockatea Shale|24443|5|Briefly described|p22, Fig.30|Middle Triassic|Early Triassic|Conformably overlies Wittecarra Sandstone, Beekeeper Formation, Dongara Sandstone and Wagina Sandstone. Conformably overlain by Woodada Formation. Geological Province: Perth Basin.||||||
9696|Kockatea Shale|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
9696|Kockatea Shale|29693|6|Mentioned|Fig.7|||||||||
9696|Kockatea Shale|29721|6|Mentioned|Table 226|||||||||
9696|Kockatea Shale|29790|6|Mentioned|p91|||||||||
9696|Kockatea Shale|30186|6|Mentioned|p104|||Cyzicus minuta occurrence||||||
9696|Kockatea Shale|30455|6|Mentioned|p24|||Triassic age||||||
9696|Kockatea Shale|30458|6|Mentioned|p21|||Lower Triassic age||||||
9696|Kockatea Shale|30460|6|Mentioned|p8|||p2,25,26. Lower Triassic age||||||27-AUG-18
9696|Kockatea Shale|30466|6|Mentioned|p5|||Lower Triassic age||||||
9696|Kockatea Shale|30547|6|Mentioned|p426|||Correlation||||||
9696|Kockatea Shale|30550|6|Mentioned|p82|||Lower Triassic age||||||
9696|Kockatea Shale|30565|6|Mentioned|Fig.4|||||||||
9696|Kockatea Shale|30948|6|Mentioned|Map legend|Scythian|Scythian|||||||
9696|Kockatea Shale|31051|6|Mentioned|p80|||||||||
9696|Kockatea Shale|31238|6|Mentioned|p28|||See also Fig. 12A||||||
9696|Kockatea Shale|31276|6|Mentioned|p144|||Refers Evans (1966). Palynology||||||
9696|Kockatea Shale|31394|5|Briefly described|p60|||L. Triassic||||||22-JUL-09
9696|Kockatea Shale|31396|6|Mentioned|p1183|||See also p1184.||||||27-AUG-18
9696|Kockatea Shale|31561|5|Briefly described|p18|||See also Section p22, map p24.||||||27-AUG-18
9696|Kockatea Shale|31562|6|Mentioned|p10|||Stratigraphic Table.||||||27-AUG-18
9696|Kockatea Shale|31568|5|Briefly described|p18|||See also p19. L. Triassic||||||27-AUG-18
9696|Kockatea Shale|31910|4|Described|Table 1|||||||||
9696|Kockatea Shale|32163|6|Mentioned|p276|||See also p279.||||||27-AUG-18
9696|Kockatea Shale|32164|6|Mentioned|p488|||||||||
9696|Kockatea Shale|32165|4|Described|p195|||Fauna Scythian (Griesbachian - Smithian)||||||
9696|Kockatea Shale|32376|6|Mentioned|p1542|||||||||
9696|Kockatea Shale|32641|6|Mentioned|p5|||L.Triass.||||||
9696|Kockatea Shale|32642|6|Mentioned|p74|||Oil production||||||
9696|Kockatea Shale|32648|6|Mentioned|p32|||Scythian||||||
9696|Kockatea Shale|32649|4|Described|p23|||See also Table  1.||||||27-AUG-18
9696|Kockatea Shale|32650|6|Mentioned|p89|||||||||
9696|Kockatea Shale|32714|6|Mentioned|Fig.2|||See also p83.||||||27-AUG-18
9696|Kockatea Shale|32715|6|Mentioned|p1186|||Oil.||||||27-AUG-18
9696|Kockatea Shale|33022|6|Mentioned|p263|||Palaeomagnetism. See also p58.||||||27-AUG-18
9696|Kockatea Shale|33168|6|Mentioned|p114|||Re- macrofossils||||||
9696|Kockatea Shale|33386|6|Mentioned|Fig.7|||||||||
9696|Kockatea Shale|33625|6|Mentioned|Fig.8|||||||||
9696|Kockatea Shale|33627|6|Mentioned|p582|||||||||
9696|Kockatea Shale|33998|6|Mentioned|p28|||Scythian||||||
9696|Kockatea Shale|34008|2|Defined|p74|Early Triassic|Early Triassic|Correlates with Blina Shale. See also pp67,73,75,77||||||18-OCT-07
9696|Kockatea Shale|34009|6|Mentioned|Table III|||||||||
9696|Kockatea Shale|34010|6|Mentioned|Cor. chart|||L.Trias||||||
9696|Kockatea Shale|34172|6|Mentioned|p52|||Lower Triassic.||||||
9696|Kockatea Shale|34241|6|Mentioned|p404|||Earliest Triassic||||||
9696|Kockatea Shale|34274|6|Mentioned|p115|||See also pp116,117 etc. L.Triassic.||||||27-AUG-18
9696|Kockatea Shale|34287|6|Mentioned|p151|||See also p163. Triassic||||||27-AUG-18
9696|Kockatea Shale|34474|6|Mentioned|p819|||||||||
9696|Kockatea Shale|34841|6|Mentioned|p95|||||||||
9696|Kockatea Shale|34846|6|Mentioned|p23|||||||||
9696|Kockatea Shale|35280|6|Mentioned|p148|||||||||
9696|Kockatea Shale|35282|6|Mentioned|Fig.2|||||||||
9696|Kockatea Shale|35573|6|Mentioned|Fig.13|||Generalised stratigraphy - Perth Basin.||||||27-AUG-18
9696|Kockatea Shale|35653|6|Mentioned|p1093|||Discussion of stratigraphy and basin development. See also Fig.3.||||||
9696|Kockatea Shale|35873|6|Mentioned|p17|||||||||
9696|Kockatea Shale|35901|6|Mentioned|p11|||||||||
9696|Kockatea Shale|35915|6|Mentioned|p27|||||||||
9696|Kockatea Shale|35968|5|Briefly described|p63|||See also Fig.8.||||||
9696|Kockatea Shale|35983|6|Mentioned|Table 26|||||||||
9696|Kockatea Shale|36100|6|Mentioned|Fig.2|||||||||
9696|Kockatea Shale|36112|6|Mentioned|p27|||||||||
9696|Kockatea Shale|36257|6|Mentioned|Table 2.1|||||||||
9696|Kockatea Shale|36265|5|Briefly described|Fig.3.26|Early Triassic|Early Triassic|Geological province: Perth Basin.||||||04-MAR-08
9696|Kockatea Shale|36266|5|Briefly described|p150|Triassic|Triassic|Includes Dongara Sandstone Member. Geological Province: Perth Basin.||||||31-MAR-08
9696|Kockatea Shale|36293|2|Defined|p123|Triassic|Triassic|||||||
9696|Kockatea Shale|36890|3|Fully described|p237|||Includes Minchin Siltstone||||||
9696|Kockatea Shale|36899|6|Mentioned|p1092|||||||||
9696|Kockatea Shale|36911|6|Mentioned|p57|||||||||
9696|Kockatea Shale|37104|6|Mentioned|Fig.3|||||||||
9696|Kockatea Shale|37286|6|Mentioned|p30|||||||||
9696|Kockatea Shale|37308|5|Briefly described|Table 4|||||||||
9696|Kockatea Shale|37577|6|Mentioned|p77|||||||||
9696|Kockatea Shale|37610|6|Mentioned|p302|||||||||
9696|Kockatea Shale|38352|6|Mentioned|p59|||||||||
9696|Kockatea Shale|38444|6|Mentioned|p300|||||||||
9696|Kockatea Shale|38484|6|Mentioned|p6|||||||||
9696|Kockatea Shale|38486|6|Mentioned|p6|||||||||
9696|Kockatea Shale|38655|6|Mentioned|p6|||||||||
9696|Kockatea Shale|38732|6|Mentioned|p31|||||||||
9696|Kockatea Shale|38998|4|Described|p19|||||||||
9696|Kockatea Shale|39155|6|Mentioned|p18|||Barrier to groundwater flow||||||
9696|Kockatea Shale|39217|6|Mentioned|p49|||Refers Evans(1966)||||||
9696|Kockatea Shale|39261|6|Mentioned|p115|||||||||
9696|Kockatea Shale|40340|5|Briefly described|p14|||Mention p21.||||||27-AUG-18
9696|Kockatea Shale|40341|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
9696|Kockatea Shale|40617|6|Mentioned|p18|||||||||
9696|Kockatea Shale|40885|4|Described|p91|||||||||
9696|Kockatea Shale|40992|6|Mentioned|p7|||||||||
9696|Kockatea Shale|40999|6|Mentioned|p307|||||||||
9696|Kockatea Shale|41172|4|Described|p124|||||||||
9696|Kockatea Shale|41192|6|Mentioned|Fig.5|||||||||
9696|Kockatea Shale|41195|4|Described|p326|||||||||
9696|Kockatea Shale|41271|6|Mentioned|p22|||||||||
9696|Kockatea Shale|41284|5|Briefly described|p89|||||||||
9696|Kockatea Shale|41589|6|Mentioned|p118|||||||||
9696|Kockatea Shale|41728|5|Briefly described|p443|||||||||
9696|Kockatea Shale|41729|6|Mentioned|p453|||||||||
9696|Kockatea Shale|42075|5|Briefly described|Fig.7 P247|||||||||
9696|Kockatea Shale|42116|5|Briefly described|p10|||||||||
9696|Kockatea Shale|42194|6|Mentioned|p33|||||||||
9696|Kockatea Shale|42687|6|Mentioned|map legend|||||||||
9696|Kockatea Shale|42688|6|Mentioned|map legend|Triassic||||||||
9696|Kockatea Shale|43031|4|Described|p13,Fig.2|||||||||
9696|Kockatea Shale|43062|5|Briefly described|p15,Table 2,p18|||||||||
9696|Kockatea Shale|43096|6|Mentioned|p7|||||||||
9696|Kockatea Shale|43197|5|Briefly described|Map Legend||Triassic|||||||
9696|Kockatea Shale|43216|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
9696|Kockatea Shale|43217|5|Briefly described|Map Legend||Triassic|Perth Basin||||||
9696|Kockatea Shale|43296|5|Briefly described|Map Legend||Triassic|||||||
9696|Kockatea Shale|43297|4|Described|p9,Fig.3 p5.||Early Triassic|See also Table1 p7.Type section location given. Age Griesbachian to Smithian (or Scythian age.)||||||21-APR-08
9696|Kockatea Shale|43323|14|Not recorded|p71||Scythian|Microflora older than microflora in Wollar Ss.||||||
9696|Kockatea Shale|43347|4|Described|4|Early Triassic|Griesbachian|||||||
9696|Kockatea Shale|43350|14|Not recorded|p 402|||||||||
9696|Kockatea Shale|43495|4|Described|6-32||Scythian|||||||
9696|Kockatea Shale|43504|4|Described|4-10||Scythian|||||||
9696|Kockatea Shale|43705|6|Mentioned|p11||Triassic|||||||
9696|Kockatea Shale|43825|6|Mentioned|p145||Triassic|||||||
9696|Kockatea Shale|43910|14|Not recorded|p12|||||||||
9696|Kockatea Shale|43923|6|Mentioned|p23||Early Triassic|||||||
9696|Kockatea Shale|43976|6|Mentioned|p69|||Re geology||||||
9696|Kockatea Shale|44006|14|Not recorded|p65-66,68,80,88|||Contemporaneity with Blina Shale (spore data) supported by finds in both of new amphibian, Deltasaurus gen.nov.||||||
9696|Kockatea Shale|44144|4|Described|p507 Tb.4-21, p509 Fig.4-145, p510|Early Triassic|Early Triassic|See also p513-514, p523. Type Section: Kockatea Creek 28o33'10''S 115o10'10''E. Over 777m thick shallow marine sediments (with shoreline sandstone Members). Fossils include molluscs, conodonts, vertebrates and palynomorphs. A reworked Devonian ostracod was found in this unit, suggesting Devonian rocks may be present in the Dandaragan Trough-Beagle Ridge area.|||Dongara Sandstone Member, Bookara Sandstone Member.|Overlain by Woodada Formation (conformably) and Greenough Sandstone (disconformably).|Light grey, green-grey or black shale with minor siltstone and sandstone; sometimes calcareous.|
9696|Kockatea Shale|44237|14|Not recorded|p.197,199,202-213||Triassic|||||||
9696|Kockatea Shale|44307|14|Not recorded|p11,15-17|||||||||
9696|Kockatea Shale|44998|14|Not recorded|p.110,114|||Microflora & plankton similar to that of Blina Shale.||||||
9696|Kockatea Shale|46849|6|Mentioned|Fig. 6|||||||||
9696|Kockatea Shale|47173|14|Not recorded|?|||||||||
9696|Kockatea Shale|47831|14|Not recorded|?|||||||||
9696|Kockatea Shale|48614|4|Described|p1,4-6, Pl.1,8|||(H50-5,9). See also p43,46,47.||||||
9696|Kockatea Shale|48615|4|Described|p.1,3,4,6,13,14.|||On many pages. (H50-5,9).  Fig.2,4. Pl.1.||||||
9696|Kockatea Shale|48848|14|Not recorded|p.17-21|||||||||
9696|Kockatea Shale|48857|2|Defined|p.13-15|||p.7,11,19.||||||
9696|Kockatea Shale|49942|4|Described|p4 Fig.3|Middle Triassic|Early Triassic|Conformably overlies Wittecarra Sandstone. Conformably overlain by Woodada Formation. Geological Province: Gascoyne Platform.||||||
9696|Kockatea Shale|50085|5|Briefly described|p15 Fig. 8|Triassic|Triassic|Age: ~250Ma. Geological Province: Northern Perth Basin.||||||22-JUL-09
9696|Kockatea Shale|50107|5|Briefly described|Map legend|Triassic|Triassic|Geological Province: Northern Perth Basin.||||||
9696|Kockatea Shale|60118|5|Briefly described|p29|Early Triassic|Permian|Geological Province: Perth Basin.||||||
9696|Kockatea Shale|60376|4|Described|p13, p17 Fig. 4.|Early Triassic|Early Triassic|Geological Province: Perth Basin. Overlain by Arranoo Sandstone Member.||||||07-FEB-11
9696|Kockatea Shale|60377|4|Described|p61 Fig. 3, p62, p71|Scythian|Wuchiapingian|Includes: Bookara Sandstone Member, Hovea Member and Arranoo Member. Overlain by Woodada Formation. Underlain by Dongara Sandstone and Beekeeper Formation. Geological Province: Perth Basin. Marine depositional environment.||||||07-FEB-11
9696|Kockatea Shale|60384|5|Briefly described|p244, p243 Fig 2a, p254, p260 table2.|Middle Triassic|Early Triassic|Perth Basin. Minor oil shows. Fine-grained marine sediment. Fluorescence, cut, dead oil, trace oil, residual hydrocarbon.||||||
9696|Kockatea Shale|60386|5|Briefly described|p296, 297, 299|Early Triassic|Early Triassic|Perth Basin. Distal shelf/basin. Includes volcanics dated 246 +/-7 Ma.||||||
9696|Kockatea Shale|60420|5|Briefly described|p423, 425 Fig. 2|Early Triassic|Late Permian|Includes: Hovea Member.||||||
9696|Kockatea Shale|61023|5|Briefly described|p20 Fig 10|Triassic|Triassic|Main prospective source for oil in the Pert Basin. Geological Province: Perth Basin.||||||11-APR-08
9696|Kockatea Shale|61541|5|Briefly described|pp263-264, p267, p270. |Early Triassic|Late Permian|This unit is the petroleum source for the crude oils of the northern onshore Perth Basin.|||Includes Hovea Member.|||
9696|Kockatea Shale|61546|5|Briefly described|p383, p385 Fig.5, p386, p388, p392. |Early Triassic|Late Permian|Widespread; forms the regional seal in the Perth Basin. Underlying shallow normal faults sole out in this unit but do not breach it.|||Includes Hovea and Arranoo Members.|Overlies Dongara Sandstone and Beekeeper Formation. Is overlain by Woodada Formation.||
9696|Kockatea Shale|61811|4|Described|p3 Fig.2, pp19-22, p26, pp34-35, p64.|Early Triassic|Late Permian|Northern Perth Basin. Rare conchostracans occur south of Kalbarri. Type section details in Appendix 1.|||Includes Bookara Sandstone and Arranoo Members.|Overlies Northampton Complex, Dongara Sandstone and Beekeeper Formation unconformably and Wittecarra Sandstone probably conformably. Overlain by Birdrong Sandstone and disconformably by Chapman Group|Uniform clayey siltstone that contains some ferruginous layers (former soil profiles?).|
9696|Kockatea Shale|63929|6|Mentioned|p129, p131 Fig.2.|Early Triassic|Early Triassic|Perth Basin. One of the few stratigraphic intervals in Australia where ammonites occur, making them of much less use for biostratigraphy than conodonts/palynomorphs. Primarily marine sediments.||||Is overlain by Woodada Formation.||
9696|Kockatea Shale|64099|5|Briefly described|p365, p366, p367 Fig. 2|Olenekian|Wuchiapingian|Includes Hovea Member at base. Shale, micaceous siltstone, minor sandstone, limestone. Overlies Dongara Sandstone/Wagina Formation (conformably/unconformably) or Carynginia Formation (unconformably). Max thick: 1060m. Geol Prov: northern Perth Basin.||||||
9696|Kockatea Shale|64580|4|Described|map legend||Early Triassic|Shale; minor siltstone and sandstone; in places calcareous; sandstone members at base.||||||09-DEC-08
9696|Kockatea Shale|64635|5|Briefly described|p4 Fig.3, p7, p14, p15 Fig.13, p16  |Olenekian|Wuchiapingian||||Includes Bookara Sandstone Member.|Overlies the Wittecarra Sandstone. Underlies the Birdrong Sandstone and Woodada Formation.|Consists of a uniform clayey siltstone that contains some ferruginous layers.|
9696|Kockatea Shale|64769|6|Mentioned|p129 Fig. 132|Triassic|Triassic|Shale and siltstone.||||||06-MAY-09
9696|Kockatea Shale|64980|5|Briefly described|pp625-634.|Early Triassic|Early Triassic|Perth Basin. Oil source and hydrocarbon reservoir seal for Dongara Sandstone, Carynginia Formation, Irwin River Coal Measures and the intra-formational Arranoo Sandstone Member.|||Includes Arranoo Sandstone Member.|||
9696|Kockatea Shale|66124|4|Described|p169, p170 Fig.2|Olenekian|Induan|Perth Basin. Underlies Woodada Formation. Shallow-marine: shale and siltstone with some limestone and sandstone. Up to 1150m thick and generally thickens southward. Contains conodonts.||||||
9696|Kockatea Shale|67135|5|Briefly described|p5 Fig.7.|Triassic|Triassic|Perth Basin.||||Overlies Wagina and Dongara Sandstones and Beekeeper Formation. Is overlain by Woodada Formation.||
9696|Kockatea Shale|67340|6|Mentioned|p6-8, 19, 25, 50, 52-63|Early Triassic|Permian|Northern Perth Basin. Thermal rock properties. Wells in this unit used for this Report are listed.|||Bookara Sandstone Member.|||
9696|Kockatea Shale|67370|4|Described|pp315-319.|Early Triassic|Late Permian|Northern Perth Basin and southern Carnarvon Basin. Thomas and Barber (2004) extended the base of this unit into the Late Permian. Is time-transgressive onto the Northampton Block. Outcrop is sparse and weathered; detailed measured sections non-existent. Source rock for several sealed northern Perth Basin sandstone reservoirs.|||Includes Hovea, 'Indoon' and Arranoo Members.|Is overlain by Woodada Formation.||
9696|Kockatea Shale|67925|5|Briefly described|Ch4 p8 fig 2|Lower Triassic|Lower Triassic|Northern and central Perth Basin. |||Includes the Arranoo Sandstone Member.|Overlain by the Woodada Formation.||
9696|Kockatea Shale|68202|6|Mentioned|p177|Triassic|Permian|The Permian-Triassic boundary most likely occurs within the Hovea Member of this unit.|||Hovea Member.|||
9696|Kockatea Shale|69029|5|Briefly described|p313,315,330,332-333|Olenekian|Olenekian|Of Canning Basin, Perth Basin. Main gas-prone source beds in Perth Basin with TOC of >1%. May host roughly half of estimated total shale-gas resources for the Perth Basin (Kuuskraa et al., 2011).|||Includes Hovea Member.|Overlain by Woodada Formation. Underlain by Sabina Sandstone.||
9696|Kockatea Shale|69081|6|Mentioned|p735|||oil and gas produced. Geol. Prov: Perth Basin||||||
9696|Kockatea Shale|69182|5|Briefly described|Ch2 p3, Ch2 p9, Ch2 p12, Ch2 p13|Early Triassic|Late Permian|See also Ch2 p34-p42, Ch2 p44, Ch2 p46, Ch2 p47-p51, Ch2 p57, Ch2 p60-p67, Ch2 p69-p74, Ch2 p69,Ch2 p80, Ch2 p84-p88, Ch2 p92-p96, Ch2 p98, Ch2 p100-p102, Ch2 p104, Ch2 p106, Ch2 p108-p110, Ch3 p12.||||Unconformably overlies the Dongara Sandstone, Wittecarra Sandstone and the Wagina Sandstone. Interbedded with the Arranoo Sandstone. Overlain by the Woodada Formation and Lesueur Sandstone.||
9696|Kockatea Shale|69297|6|Mentioned|p202, p206, p234, p237, p247, p515|Middle Triassic|Lower Triassic|Perth Basin. Deposited in a deep marine environment.  ||||||
9696|Kockatea Shale|69788|6|Mentioned|p1034 Fig.9|Triassic|Triassic|Local basement to Tamala Limestone in Pinnacles Desert area.||||||
9696|Kockatea Shale|69840|6|Mentioned|p197 Fig.14|Triassic|Triassic|Shown only on cross-section diagram p197 Fig.14||||Underlies Tamala Limestone.|Shale.|
9696|Kockatea Shale|70065|5|Briefly described|Regional: p6|||Northern Perth Basin. Source of the onshore oil fields and offshore accumulation at Cliff Head.||||Equivalent to Locker Shale.||
9696|Kockatea Shale|70097|5|Briefly described|p2, p4, p6-8, p10, p20-22 Figs.4-6|Olenekian|Changhsingian|Extensive and rapid marine transgression throughout Perth Basin. Initial slow deposition resulted in accumulation of organic-rich sediments of Hovea Member (45.7 m thick in Lilac 1). This was followed by rapid deposition of remainder of Kockatea Shale (435 m thick in Batavia 1). Regional seal. Northern Perth Basin. Greenough/Bookara Shelf, Dongara Saddle and Dandaragan Trough.|||Hovea Member, Aranoo Sandstone Member|Overlies Irwin River Coal Measures or Wittecarra Sandstone. Is overlain by Woodada Formation.|Shale and sandstone.|12-SEP-17
9696|Kockatea Shale|70128|5|Briefly described|p449, p453, p455, p457, p459-462|Early Triassic|Early Triassic|Northern Perth Basin. Modelled thickness distribution histogram.||||Unconformably overlies Dongara and Wagina Sandstones and Beekeeper Formation. Is overlain conformably by Woodada Formation. Time-equivalent of Sabina Sandstone.||
9696|Kockatea Shale|70796|4|Described|2_5m_interpgeop15_lut.csv|Lower Triassic|Lower Triassic|Of the Perth Basin. Affected by the following events: MidMiocene transgression, 15 Ma (15 15 Ma); Wilson Bluff transgression, 42 Ma (42 42 Ma); Kings Park transgression, 56 Ma (56  56 Ma); Gondwana breakup  western margin (210  125 Ma); Jurassic  Early Cretaceous rifting, Perth Basin (168  133 Ma). See also 500k_interpgeop14_lut.csv.|252.17  247.2 Ma (biostrat)||||Shale; minor siltstone and sandstone; in places calcareous; sandstone members at base.|
9696|Kockatea Shale|70826|6|Mentioned|p7 tbl 4|Triassic|Triassic|Perth Basin.||||||
9696|Kockatea Shale|71146|5|Briefly described|p6,  p43 fig 33|Early Triassic|Lopingian|Perth Basin.||||Overlies the Wagina-Dongara Sandstone. Overlain by the Woodada Formation.|Shale.|
9696|Kockatea Shale|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, shale|
9696|Kockatea Shale|71269|4|Described|GEOL_LUT_CSV files|Early Triassic|Early Triassic|Of Perth Basin. Events: Mid-Miocene transgression, 15 Ma (15-15 Ma); Wilson Bluff transgression, 42 Ma (42-42 Ma); Kings Park transgression, 56 Ma (56-56 Ma); Gondwana breakup-western margin (210-125 Ma); Jurassic-Early Cretaceous rifting, Perth Basin (168-133 Ma);??.  See 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|252.17-247.2 Ma (biostrat)||||Shale; minor siltstone and sandstone; in places calcareous; sandstone members at base|
9696|Kockatea Shale|71377|6|Mentioned|p77|Lower Triassic|Lower Triassic|Perth Basin. Deposited in a marine environment. Equivalence to the Sabina Sandstone is interpreted on the basis of palynologyical evidence.||||Equivalent to the Sabina Sandstone.||
9696|Kockatea Shale|71623|6|Mentioned|p355, p345 fig 2, p349 Fig 7, p350, 354||Scythian|Perth Basin. Early Triassic.|||||Shale|
9696|Kockatea Shale|72034|5|Briefly described|500k_interpgeop16_lut|Early Triassic|Early Triassic|Perth Basin.  Age from biostratigraphy.|||||Shale; minor siltstone and sandstone; in places calcareous; sandstone members at base.|
9696|Kockatea Shale|72258|5|Briefly described|p129,133-135|Early Triassic|Early Triassic|Of Perth Basin. Minor distribution of Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Major peak in Mesoproterozoic (1300-1100 Ma) and minor Late Paleoproterozoic (1800-1600 Ma) detrital zircons correlate with characteristic ages and Hf isotopic signatures of magmatism in the Albany-Fraser-Wilkes Orogen (Clark et al., 2000; Fitzsimons, 2000, 2003; Kirkland et al., 2011; Spaggiari et al., 2015). Late Meso- to Early Neoproterozoic (1100-900 Ma) detrital zircons atributed to Pinjarra Orogen.||||Overlain by Woodada Formation. Underlain by Dongara Sandstone. Laterally grades into Sabina Sandstone.||
9696|Kockatea Shale|72505|5|Briefly described|p890|Induan|Changhsingian|Perth Basin. Correlates with the P. Microcorpus and P. Crenulata zones.|||Includes the Hovea Member.|Overlies the Beekeeper Formation, Dongara Sandstone and the Wagina Sandstone.||
9696|Kockatea Shale|72910|6|Mentioned|p4 Fig.3.|Triassic|Triassic|Shown as being located in the Northern Perth Basin.||||Overlies Wagina Sandstone, Dongara Sandstone and Beekeeper Formation.||
9696|Kockatea Shale|73304|6|Mentioned|p77|||Shown as Kockatea Shale Formation p71.||||||
9696|Kockatea Shale|73484|5|Briefly described|p473, p476-478, p480-482, p486-488, p491|Early Triassic|Early Triassic|Perth Basin. Marine. Onlaps Northampton Complex. Deposited in a rapid regional marine transgression. Contains Olenekian ammonoid fossils (Chen et al., 2012, 2014). See also p475 Fig.2.|||Hovea Member|Overlies Hovea Member, Northampton Complex|Alternating beds of finely laminated claystone and siltstone to fine-grained sandstone. Siltstones contain ichnofauna and microbially induced sedimentary structures.|
9696|Kockatea Shale|73513|5|Briefly described|p29, p30 Fig.2, p32, p39|Scythian|Tatarian|Perth Basin. Deposited in a major regional transgression. Major regional seal. Misspelt as Kockatea Formation p39.|||Hovea Member|Overlies Dongara Sandstone, underlies Woodada Formation|Marine rocks.|
9714|Kojonup Sandstone|22769|5|Briefly described|Table1p759||Late Eocene|||||||
9714|Kojonup Sandstone|23880|5|Briefly described|p42|Eocene|Eocene|Geological Province: Yilgarn Craton.||||||
9714|Kojonup Sandstone|30268|6|Mentioned|p42|||||||||
9714|Kojonup Sandstone|31562|6|Mentioned|p10|||Stratigraphic Table.||||||
9714|Kojonup Sandstone|33801|4|Described|p49|||||||||
9714|Kojonup Sandstone|36890|3|Fully described|p432|||||||||
9714|Kojonup Sandstone|37341|4|Described|p232|||||||||
9714|Kojonup Sandstone|37350|6|Mentioned|Fig.1|||||||||
9714|Kojonup Sandstone|40358|6|Mentioned|p24|||||||||
9714|Kojonup Sandstone|40359|4|Described|p24|||||||||
9714|Kojonup Sandstone|40360|6|Mentioned|Map legend|Eocene|Eocene|Prob. Eocene||||||
9714|Kojonup Sandstone|40927|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
9714|Kojonup Sandstone|40928|4|Described|p13|||||||||
9714|Kojonup Sandstone|42396|6|Mentioned|p4|||||||||
9714|Kojonup Sandstone|61155|5|Briefly described|p17|Late Eocene|Middle Eocene|Geological region: Darling Range. ||||||
9760|Kongorow Granite|23722|5|Briefly described|p11|||Now part of Lennard Granite?||||||
9760|Kongorow Granite|30097|6|Mentioned|Table 27|||||||||
9760|Kongorow Granite|30525|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9760|Kongorow Granite|30533|4|Described|p12|||On Table 1||||||
9760|Kongorow Granite|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9760|Kongorow Granite|30896|4|Described|p13|||Lower Proterozoic||||||
9760|Kongorow Granite|30897|6|Mentioned|p10|||On stratigraphic table||||||
9760|Kongorow Granite|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
9760|Kongorow Granite|31226|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
9760|Kongorow Granite|32660|5|Briefly described|Table 1|||||||||
9760|Kongorow Granite|32728|4|Described|p21|||See also Fig.3||||||
9760|Kongorow Granite|36885|4|Described|p170|||||||||
9760|Kongorow Granite|37462|4|Described|Table 4.I|||See also Fig.4.6||||||
9760|Kongorow Granite|38482|6|Mentioned|Table 1|||||||||
9760|Kongorow Granite|41158|6|Mentioned|Plate 2|||||||||
9760|Kongorow Granite|41987|6|Mentioned|p70|||||||||
9760|Kongorow Granite|42149|6|Mentioned|p704|||||||||
9760|Kongorow Granite|42710|5|Briefly described|map legend|Proterozoic||||||||
9760|Kongorow Granite|42811|4|Described|p8|||||||||
9760|Kongorow Granite|42814|5|Briefly described|p8|||||||||
9760|Kongorow Granite|43281|5|Briefly described|Map legend||Proterozoic|||||||
9760|Kongorow Granite|44155|5|Briefly described|p234 Tb.3-2, p239-240, p247, p248 Tb.3-8|Paleoproterozoic|Paleoproterozoic|West Kimberley. Intermittent intrusions as a number of phases. Stratigraphic position uncertain.||Hooper Complex.||Intrudes Halls Creek Group.|Foliated porphyritic biotite syenogranite, and granodiorite; garnet-bearing, gneiss bands locally; deformed.|
9760|Kongorow Granite|48931|3|Fully described|p42|||||||||
9760|Kongorow Granite|50437|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Paperbark Supersuite. Age: 1852 +/- 4Ma (Shrimp).  See also the misspelt Kongrow Granite.||||||07-NOV-08
9760|Kongorow Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1852 Ma|Paperbark Supersuite||||
9760|Kongorow Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This is a reliable age for igneous crystallisation of the granite, close to the 1854 Ma age of the Whitewater Volcs, but about 10 m.y. younger than other West Kimb. granites.'|1852+/-4 Ma U/Pb SHRIMP|Paperbark Supersuite|||Foliated, porphyritic, biotite-rich metamonzogranite and metagranodiorite; contains mafic inclusions and mafic bands.|31-JUL-15
9760|Kongorow Granite|69165|6|Mentioned|GA_geochron.csv|Paleoproterozoic|Neoarchean||1852-2507 Ma|||||
9760|Kongorow Granite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone. See 250k_geologyp_lut.csv, 250k_interpgeop_lut.csv.|1852 Ma (isotopic)|Unit of Paperbark Supersuite.|||Foliated, porphyritic, biotite-rich metamonzogranite and metagranodiorite; contains mafic inclusions and mafic bands|
9760|Kongorow Granite|69660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Kimberley Craton.|c.1852 Ma; Griffin et al. (2000).|Unit in Paperbark Supersuite.|||Foliated, porphyritic, biotite-rich metamonzogranite and metagranodiorite; contains mafic inclusions and mafic bands.|
9760|Kongorow Granite|70154|5|Briefly described|250k_geologyp_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 250k_interpgeop_lut.csv.|1852 Ma||||Foliated, porphyritic, biotite-rich metamonzogranite and metagranodiorite; contains mafic inclusions and mafic bands|
9760|Kongorow Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 250k_geologyp_lut.csv, 1m_interpgeop_lut.csv.|1852+\-4 Ma (isotopic)|Unit of Paperbark Supersuite.|||Foliated porphyritic biotite-rich monzogranite and granodiorite with mafic xenoliths and gneissic bands|
9760|Kongorow Granite|72437|5|Briefly described|p62, p64-65, p77|||Hooper Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated granodiorite and monzogranite.|
9766|Kookhabinna Sandstone|29845|6|Mentioned|Table 69|||||||||
9768|Koolan Island iron formation|39948|6|Mentioned|Fig.2|||||||||
9769|Koolanooka Porphyry|40346|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
9769|Koolanooka Porphyry|40347|6|Mentioned|p5|||See also P14||||||
9789|Koomberan Greywacke|23815|5|Briefly described|p279|Sakmarian|Sakmarian|Geological Province: Carnarvon Basin. Of the Lyons Group. Underlying unit: Dumbardo Siltstone. Overlying unit: Mundarie Siltstone.||||||
9789|Koomberan Greywacke|32648|6|Mentioned|p32|||Lyons Gp.||||||
9789|Koomberan Greywacke|36890|6|Mentioned|p279|||||||||
9789|Koomberan Greywacke|37295|6|Mentioned|Table 2|||||||||
9789|Koomberan Greywacke|41271|6|Mentioned|p65|||||||||
9789|Koomberan Greywacke|44344|14|Not recorded|p.6-9,22,24||Sakmarian|Sakmarian. (G50-1). opp.4, map.||||||
9789|Koomberan Greywacke|44345|14|Not recorded|map legend||Sakmarian|||||||
9789|Koomberan Greywacke|44532|14|Not recorded|p.5, map|||(G50-5).||||||
9789|Koomberan Greywacke|44533|5|Briefly described|map legend||Sakmarian|Sakmarian.||||||
9789|Koomberan Greywacke|45015|5|Briefly described|map legend|Sakmarian|Sakmarian|Of the Lyons Group. Geological Province: Carnarvon Basin.||||||31-MAY-06
9789|Koomberan Greywacke|45016|2|Defined|p36-38||Sakmarian|Tb, p.7,9,12,13,15,16,32,34,35,39,40,43,67,Fig.50,52. (F50-13 type area).||||||
9789|Koomberan Greywacke|61958|5|Briefly described|Map sheet 1|Sakmarian|Sakmarian|||||||
9793|Koongie Park Formation|22474|5|Briefly described|p20|Orosirian|Orosirian|1843 +/- 3 Ma||||||
9793|Koongie Park Formation|22496|5|Briefly described|p8|Orosirian|Paleoproterozoic|c. 1843 Ma||||||07-NOV-08
9793|Koongie Park Formation|22526|6|Mentioned|Fig2 P681, Fig3||Orosirian|||||||
9793|Koongie Park Formation|22547|5|Briefly described|P8|Orosirian|Orosirian|Age: 1845-1840 Ma. Overlies Tickalara Metamorphics.||||||14-NOV-06
9793|Koongie Park Formation|22716|5|Briefly described|table4, p232,234,236|Orosirian|Orosirian|Age: 1840Ma||||||
9793|Koongie Park Formation|22754|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Tightly folded, low- to medium-grade, felsic volcaniclastic rocks and lavas; pelitic to psammitic epiclastic rocks; mafic volcanic rocks, interbedded chert , BIF and carbonate rock. Age c.1845-1840 Ma (SHRIMP). Dominates Central zone of Lamboo Complex.||||||07-NOV-08
9793|Koongie Park Formation|23383|5|Briefly described|p9, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Lamboo Complex. On ANGELO this unit includes rocks formerly mapped as Tickalara metamorphics.  Intruded by the Loadstone and Dillinger Monzogranites and Angelo Microgranite. Geological Province: Hooper Complex.  See also p6 Fig. 3.||||||07-NOV-08
9793|Koongie Park Formation|23568|5|Briefly described|p2777 Fig 2|Paleoproterozoic|Paleoproterozoic|Age: ~1845-1800 Ma.||||||07-NOV-08
9793|Koongie Park Formation|23599|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Age: c.1845 Ma. Geological Province: Lamboo Complex.||||||07-NOV-08
9793|Koongie Park Formation|23601|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed felsic and volcaniclastic rocks; minor chert, banded-iron formation and carbonate.||||||07-NOV-08
9793|Koongie Park Formation|23621|2|Defined|p53 Appendix|Orosirian|Orosirian|See also page 19, 11 table 1. Age: 1843+/-2 Ma (U-Pb zircons). Overlain by Moola Bulla Formation. Geological Province: Halls Creek Orogen. Max. thickness: >1000 m.||||||09-DEC-08
9793|Koongie Park Formation|23622|5|Briefly described|Map Legend|Orosirian|Orosirian|Age: c 1843 Ma.||||||
9793|Koongie Park Formation|23925|5|Briefly described|p220 Fig. 2|Orosirian|Orosirian|Age: c. 1845Ma. Geological Province: Halls Creek Orogen.||||||
9793|Koongie Park Formation|24173|3|Fully described|p19, p12 Tb.2|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Moola Bulla Fm. Geol.Prov: Halls Creek Orogen. Max Thickness: >1000m. Age: 1843 +/- 2Ma. Previously mapped as Biscay and Olympio Fms. by Gemuts & Smith (1968); also referred to as Koongie Park Member of Tickalara Metamorphics.||||||07-NOV-08
9793|Koongie Park Formation|24197|5|Briefly described|p86, p90 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Koongie Park Suite. Volcanics deposited in a subaqueous environment. Age: 1840Ma. Geological province: Kimberley Province.||||||07-FEB-11
9793|Koongie Park Formation|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex.  metamorphosed felsic volcanic and volcaniclastic rocks, metasedimentary rock, metabasalt and hornfels; locally migmatitic.  Age: c.1843Ma.||||||07-NOV-08
9793|Koongie Park Formation|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
9793|Koongie Park Formation|42768|4|Described|p6, Fig.6|||Radiometric age of 1843 +/- 2 Ma. Part of the Lamboo Complex. Reserved as Koongie Park Member.||||||14-NOV-06
9793|Koongie Park Formation|43561|6|Mentioned|p1437|||Erupted approx 1840 Ma||||||
9793|Koongie Park Formation|43610|5|Briefly described|p19|||Age: 1843+/-2 Ma (Zircon, Page et al,1994)||||||
9793|Koongie Park Formation|43854|5|Briefly described|Map Legend||Proterozoic|||||||
9793|Koongie Park Formation|43931|5|Briefly described|p20||Orosirian|1843 +/- 3 Ma||||||
9793|Koongie Park Formation|44231|5|Briefly described|Map Legend||Proterozoic|Metamorphosed felsic volcanic and volcaniclastic rocks; minor chert, banded-iron formation, and carbonate. Age: c.1845Ma. Of the Lamboo Complex.||||||19-MAY-05
9793|Koongie Park Formation|44693|5|Briefly described|Map Legend||Proterozoic|||||||
9793|Koongie Park Formation|44694|5|Briefly described|Map Legend||Proterozoic|||||||
9793|Koongie Park Formation|44868|5|Briefly described|Map Legend||Proterozoic|||||||
9793|Koongie Park Formation|50437|5|Briefly described|p1.6, 5.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region.  Of the Koongie Park Suite. Age: 1845-1840 +/- 4Ma (Shrimp). Used interchangeably with Koongie Park Suite.||||||09-DEC-08
9793|Koongie Park Formation|60283|6|Mentioned|p25 Fig.2|||Halls Creek Orogen.||||||
9793|Koongie Park Formation|61056|6|Mentioned|p786|Paleoproterozoic|Paleoproterozoic|See also Kongee Park Formation.||||||07-NOV-08
9793|Koongie Park Formation|63866|4|Described|p129, p131-p132, p138|Orosirian|Orosirian|Central Zone, Halls Creek Orogen. Hosts a sub-economic Zn-Cu-Pb VMS deposit. Numeric age range interpreted as extrusion ages of the rhyolites of this formation.|c. 1845-1840 Ma (Page and Sun, 1994)|||Unconformably overlain by the Moola Bulla Formation and the Kimberley Group.|Turbidite sequences, volcaniclastics, shale, chert, basalt and rhyolite.|
9793|Koongie Park Formation|64572|6|Mentioned|p802 Fig. 4|Paleoproterozoic|Paleoproterozoic|Age: ~1845Ma.||||||22-DEC-08
9793|Koongie Park Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed felsic volcanic and volcaniclastic rocks, metasedimentary rocks, metabasalt, and hornfels;  locally migmatitic; minor chert, banded iron-formation, and carbonate; locally intimately veined by granitic rocks and gabbro.||||||09-DEC-08
9793|Koongie Park Formation|65413|6|Mentioned|p105 Fig.1.|Paleoproterozoic|Paleoproterozoic|||Unit in Lamboo Complex.||||
9793|Koongie Park Formation|66845|5|Briefly described|p536 Fig.2, p537|Paleoproterozoic|Paleoproterozoic|Central zone of Lamboo Complex. Sedimentary and volcanic rocks deposited at 1845-1840 Ma (Page et al. 1994).|c. 1843 Ma|||||
9793|Koongie Park Formation|66846|6|Mentioned|p549 Fig.2|Orosirian|Orosirian|In the Central Zone of the Lamboo Complex.|||||Felsic and mafic volcanic rock.|
9793|Koongie Park Formation|68078|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|Deposited in a rifted continental arc setting.|1845-1840 Ma||||Sediments and felsic/mafic volcanic rocks.|
9793|Koongie Park Formation|68656|5|Briefly described|GEOL_LUT_CSV/500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed felsic volcanic and volcaniclastic rocks, metasedimentary rocks, metabasalt, and hornfels;  locally migmatitic; minor chert, banded iron-formation, and carbonate; locally intimately veined by granitic rocks and gabbro.|
9793|Koongie Park Formation|69003|5|Briefly described|p5, p19|||Central zone, Lamboo Province, Halls Creek Orogen.|c.1845-c.1840 Ma.||||Sedimentary and volcanic rocks.|
9793|Koongie Park Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This age for one of the Koongie Park Formation volcanics .. is a reliable stratigraphic age, in excellent agreement with the other results from this volcanic unit.'|1840+/-4 Ma, 1845+/-3 Ma U/Pb SHRIMP||Includes Angelo Microgranite[?], Onedin Member and 7 unnamed members.||Low- to high-grade felsic metavolcanic and metavolcaniclastic rock, metasedimentary rock, metabasalt, and hornfels; locally migmatitic; minor metachert, meta banded iron-formation, and metacarbonate|31-JUL-15
9793|Koongie Park Formation|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_geologyp08_lut.csv. |1845 Ma||Includes Angelo Microgranite, Onedin Member||Low- to high-grade felsic metavolcanic and metavolcaniclastic rock, hornfelsed metasedimentary rock, metabasalt, and hornfels;  locally migmatitic; minor metachert, meta banded iron-formation, and metacarbonate.|
9793|Koongie Park Formation|69585|5|Briefly described|p4-5|Orosirian|Orosirian|Central Lamboo Province. Interpreted as a rifted arc succession.|1845-1840 Ma.||||Sedimentary and mafic and felsic volcanics.|
9793|Koongie Park Formation|69587|5|Briefly described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed felsic volcanic and volcaniclastic rocks, metasedimentary rocks, metabasalt, and hornfels;  locally migmatitic; minor chert, banded iron-formation, and carbonate; locally intimately veined by granitic rocks and gabbro|
9793|Koongie Park Formation|69597|5|Briefly described|p3, p5 fig 2b|Paleoproterozoic|Paleoproterozoic|Central Lamboo Province. Possibly formed in a rifted-arc or back arc environment. |1843 Ma||||Sedimentary rocks.|
9793|Koongie Park Formation|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Central Zone. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1845-1840 Ma (Isotopic)||Includes Angelo Microgranite, Onedin Member.||Felsic metavolcanicn metavolcaniclastic rock, metarhyolite to metadacite sheet-like intrusions, minor metadolerite sills, interbedded pelite, metabasalt, and hornfels;  locally migmatitic; minor metachert, metamorphosed BIF, and metacarbonate.|
9793|Koongie Park Formation|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1840-1845 Ma||Includes Onedin Member||Low to high grade felsic metavolcanic and metavolcaniclastic rock, metasedimentary rock, metabasalt and meta hornfels, minor metachert and meta banded iron formations.|
9793|Koongie Park Formation|70731|6|Mentioned|p268-269,278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton. Associated with rfiting of underlying Tickalara Metamorphics c. 1845-1840 Ma.||||||
9793|Koongie Park Formation|70812|5|Briefly described|p6, p8, p11, p13, p20|Orosirian|Orosirian|Western Zone of the Halls Creek Orogen, Lamboo Province. Mineralisation and prospectivity are described. See also p22, p25, p27, p30, p38, p43.|c. 1850 Ma||Includes the Onedin Member and Angelo Microgranite.|||
9793|Koongie Park Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|||||||
9793|Koongie Park Formation|70851|5|Briefly described|p3-p5, p24, p29|||Central Zone, Lamboo Province. Geophysical response is briefly discussed.|c. 1845-1840 Ma||||Sedimentary, mafic and felsic volcanic rocks.|
9793|Koongie Park Formation|71113|5|Briefly described|p96, p98-100|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen.  Exposed in the southern part of the Central Zone. Deposition resulted from rifting of Tickalara Metamorphics at 1845-1840 Ma at the end of the Hooper Orogeny (Typer et al., 2012).|1845-1840 Ma||||Folded and metamorphosed turbidites, carbonates, mafic and felsic volcaniclastic rocks.|21-AUG-19
9793|Koongie Park Formation|71140|6|Mentioned|p96, 98, 100|Orosirian|Orosirian|Central Zone, Lamboo Province, Halls Creek Orogen. Resulted from rifting of the Tickalara Metamorphics.|1845-1840 Ma (deposition).||||A sequence of folded and metamorphosed turbidites, carbonates, mafic and felsic volcanic/volcaniclastic rocks.|
9793|Koongie Park Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1845+\-3 to 1840+\-4 Ma (Isotopic)||Includes Angelo Microgranite and Onedin Member.||Metamorphosed felsic volcanic and volcaniclastic rocks, metasedimentary rocks, metabasalt, and hornfels; locally migmatitic; minor chert, banded iron-formation, and carbonate; locally intimately veined by granitic rocks and gabbro|
9793|Koongie Park Formation|71397|5|Briefly described|p4-6|Orosirian|Orosirian|Geological province: Central Zone, Lamboo Province, Halls Creek Orogen. Associated with 1845-1840 Ma back-arc or arc extension in southern extent of Central Zone. Includes clasts of metamorphic and granitic rocks indicating a continental source. Metamorphosed to greenschist facies accompanied by folding, and subsequently intruded by Kevins Dam Suite during 1832-1808 Ma Halls Creek Orogeny. Hosts mafic-ultramafic layered intrusions; Page and Hoatson (2000) identified three main episodes at c. 1855 Ma, 1845 Ma and 1830 Ma.|c. 1845-1840 Ma||||Marine sedimentary rocks and bimodal volcanic and volcaniclastic rocks.|
9793|Koongie Park Formation|71873|5|Briefly described|p426,442-444|Orosirian|Orosirian|Geological province: Lamboo Province. Also referred to as Koongie Park volcanics in text. Felsic volcanism and marine sedimentation in the southern Central Zone at 1845-1840 Ma (Orth 2002; Page et al., 1994), associated with Zn-Pb VMS mineralisation. Coeval with Dougalls Suite.|1845-1840 Ma|||Intruded by Kevins Dam Suite.||
9793|Koongie Park Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Central Zone, Halls Creek Orogen.|Max age 1845+/-3 Ma. Min 1840+/-4 Ma.||||Low- to high-grade felsic metavolcanic and metavolcaniclastic rock, metasedimentary rock, metabasalt, and hornfels;  locally migmatitic; minor metachert, metamorphosed banded iron-formation, and metacarbonate.|
9793|Koongie Park Formation|72437|5|Briefly described|p6, p48-49|Palaeoproterozoic|Palaeoproterozoic|Originally thought to be dominated by felsic volcanic rocks (Griffin and Tyler, 1992b; Sheppard et al, 1995) but now includes mafic volcanic and metasedimentary rocks.|c. 1845-1840 Ma||||Felsic meta-volcanic rocks, felsic schist, microgranite, metarhyolite, banded rhyolite and metabasalt.|
9823|Korojon Calcarenite|12729|6|Mentioned|p.17||Cretaceous|Deposited in a moderate-energy marine environment. Maximum thickness penetrated was 80 m in Quobba 1 (110-190 m).||||Conformably overlies the Toolonga Calcilutite (gradational); disconformably underlies the Miria Formation.|Silty calcarenite and calcisiltite with abundant fragments of the bivalve Inoceramus.|
9823|Korojon Calcarenite|13615|6|Mentioned|p72|||||||||
9823|Korojon Calcarenite|14228|5|Briefly described|p5 Fig.2, p9, p16|Cretaceous|Cretaceous|Up to 80 m thick.||||Grades down into Toolonga Calcilutite. Overlain disconformably by Miria Formation.|Silty calcarenite and calcisiltite.|
9823|Korojon Calcarenite|23311|5|Briefly described|map legend|Late Cretaceous|Late Cretaceous|||||||
9823|Korojon Calcarenite|23403|4|Described|p9|Cretaceous|Cretaceous|||||||24-NOV-09
9823|Korojon Calcarenite|23520|5|Briefly described|p6 Fig. 4|Late Cretaceous|Late Cretaceous|Geological Province: Abrolhos Sub-basin.  See also p12.||||||
9823|Korojon Calcarenite|23620|5|Briefly described|p4 Fig. 4|Cretaceous|Cretaceous|Predominantly calcareous pelagic deposits||||||
9823|Korojon Calcarenite|23726|6|Mentioned|p11|||Geological Province: Carnarvon Basin.||||||
9823|Korojon Calcarenite|23815|4|Described|p298|Maastrichtian|Campanian|Geological Province: Carnarvon Basin. Overlying unit: Miria Marl (disconformable). Underlying unit: Toolonga Calcilutite (conformable). Max. thicknes: 45 m. Fossiliferous.||||||27-APR-05
9823|Korojon Calcarenite|23915|5|Briefly described|p518 Table 1|Late Cretaceous|Late Cretaceous|Geological Province: Southern Carnarvon Basin.||||||
9823|Korojon Calcarenite|23976|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
9823|Korojon Calcarenite|23977|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
9823|Korojon Calcarenite|23978|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
9823|Korojon Calcarenite|24059|5|Briefly described|p138|Late Cretaceous|Late Cretaceous|Geological Province: Exmouth Sub-basin.||||||
9823|Korojon Calcarenite|24094|4|Described|p268, p275|Maastrichtian|Campanian|Overlies Toolonga Calcilutite, overlain disconformably by Miria Formation.||||||
9823|Korojon Calcarenite|24351|5|Briefly described|Plate 3, Plate 4 (in pocket)|Late Cretaceous|Late Cretaceous|Geological Province: Exmouth Sub-basin. Log Houtman-1 and Log Wittecarra-1.||||||13-DEC-07
9823|Korojon Calcarenite|29381|4|Described|p68|||||||||
9823|Korojon Calcarenite|30875|6|Mentioned|p10|||See also p13. Senonian.||||||24-AUG-18
9823|Korojon Calcarenite|31396|6|Mentioned|p1183|||See also p1184.||||||24-AUG-18
9823|Korojon Calcarenite|32648|6|Mentioned|p32|||U. Cret.||||||
9823|Korojon Calcarenite|32979|6|Mentioned|p38|||Correlations with basins in India.||||||
9823|Korojon Calcarenite|33165|6|Mentioned|Chart|||Correlation chart only||||||
9823|Korojon Calcarenite|34343|5|Briefly described|p97|||See also p98. Maastrichtian.||||||24-AUG-18
9823|Korojon Calcarenite|34363|6|Mentioned|p56|||See also Fig.7. Campanian.||||||
9823|Korojon Calcarenite|34838|6|Mentioned|p3|||||||||
9823|Korojon Calcarenite|35105|6|Mentioned|Fig.5|||||||||
9823|Korojon Calcarenite|36257|6|Mentioned|Table 2.1|||||||||
9823|Korojon Calcarenite|36305|6|Mentioned|p353|||||||||
9823|Korojon Calcarenite|36890|3|Fully described|p298|||||||||
9823|Korojon Calcarenite|37016|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
9823|Korojon Calcarenite|38444|6|Mentioned|p300|||||||||
9823|Korojon Calcarenite|39170|6|Mentioned|Fig.48|||Sonic and pseudovelocity data for Pendock NO.1||||||
9823|Korojon Calcarenite|39427|4|Described|Table 1|||||||||
9823|Korojon Calcarenite|40144|6|Mentioned|p306|||||||||
9823|Korojon Calcarenite|40617|6|Mentioned|p15|||||||||
9823|Korojon Calcarenite|40800|6|Mentioned|p10|||||||||
9823|Korojon Calcarenite|40801|6|Mentioned|p42|||||||||
9823|Korojon Calcarenite|41172|6|Mentioned|p129|||||||||
9823|Korojon Calcarenite|41271|3|Fully described|p159|||||||||
9823|Korojon Calcarenite|41280|4|Described|p144|||||||||
9823|Korojon Calcarenite|41422|6|Mentioned|Fig.2|||||||||
9823|Korojon Calcarenite|41438|6|Mentioned|p109|||||||||
9823|Korojon Calcarenite|41439|6|Mentioned|p123|||||||||
9823|Korojon Calcarenite|41444|6|Mentioned|Fig.4|||||||||
9823|Korojon Calcarenite|41522|6|Mentioned|Plate 1|||||||||
9823|Korojon Calcarenite|41712|6|Mentioned|Fig.8|||||||||
9823|Korojon Calcarenite|42116|5|Briefly described|Fig.1 P6|||||||||
9823|Korojon Calcarenite|42123|4|Described|p35|||||||||
9823|Korojon Calcarenite|42563|5|Briefly described|p133, 166|||||||||
9823|Korojon Calcarenite|42995|4|Described|p35|||see also Table 1||||||
9823|Korojon Calcarenite|43564|6|Mentioned|Fig.2,p446|Maastrichtian|Campanian|||||||
9823|Korojon Calcarenite|43712|5|Briefly described|p12||Cretaceous|||||||
9823|Korojon Calcarenite|43722|6|Mentioned|p11||Cretaceous|||||||
9823|Korojon Calcarenite|43724|5|Briefly described|p30||Cretaceous|||||||
9823|Korojon Calcarenite|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||01-MAR-10
9823|Korojon Calcarenite|44344|14|Not recorded|p.18,20,24,opp.4,map|Maastrichtian|Campanian|Fm of Cardabia Group. Campanian-L.Maastrichtian in age. (G50-1).||||||24-AUG-18
9823|Korojon Calcarenite|44345|14|Not recorded|map legend||Late Cretaceous|Upper Cretaceous.||||||
9823|Korojon Calcarenite|44537|14|Not recorded|map legend||Late Cretaceous|Upper Cretaceous.||||||
9823|Korojon Calcarenite|44657|14|Not recorded|p.5,6,12,15|||||||||
9823|Korojon Calcarenite|44996|14|Not recorded|p.10-12,15|||Underlies Miria Marl p.16,54.||||||
9823|Korojon Calcarenite|45015|5|Briefly described|map legend|Late Cretaceous|Late Cretaceous|Geological Province: Carnarvon Basin.||||||31-MAY-06
9823|Korojon Calcarenite|48610|14|Not recorded|p15,Pl.1,5,6|||Salt Marsh area.||||||
9823|Korojon Calcarenite|48616|14|Not recorded|p.1,10,11 Pl.1.|||||||||
9823|Korojon Calcarenite|48831|14|Not recorded|p.10,11,19,20,32|||||||||
9823|Korojon Calcarenite|48861|2|Defined|p.5,6|||p.1. Pl.1.||||||
9823|Korojon Calcarenite|48925|6|Mentioned|p34|Campanian||||||||
9823|Korojon Calcarenite|49942|4|Described|p4 Fig.3, p11|Late Cretaceous|Late Cretaceous|Conformably overlies Toolonga Calcilutite. Unconformably overlain by Miria Marl. Max. thickness: 80 m. Geological Province: Gascoyne Platform.||||||
9823|Korojon Calcarenite|60384|6|Mentioned|p243 Fig 2a|Late Cretaceous|Late Cretaceous|Carnarvon Basin.||||||
9823|Korojon Calcarenite|60709|5|Briefly described|p830, 859|Maastrichtian|Campanian|Geological Province: Southern Carnarvon Basin.||||||
9823|Korojon Calcarenite|61958|5|Briefly described|Map sheet 1|Late Cretaceous|Late Cretaceous|||||||
9823|Korojon Calcarenite|62734|5|Briefly described|p1362 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Barrow Sub-basin.||||||01-SEP-08
9823|Korojon Calcarenite|62837|5|Briefly described|Stratigraphic columns|Maastrichtian|Maastrichtian|Age: >70Ma. Geological Province: Exmouth, Barrow and Dampier Sub-basins.||||||01-MAR-10
9823|Korojon Calcarenite|63068|5|Briefly described|p44 Fig. 2|Maastrichtian|Campanian|Geological Province: Carnarvon Basin.||||||
9823|Korojon Calcarenite|67200|6|Mentioned|p17 table 1|||Thermal conductivity of 1.68 W/mK||||||
9823|Korojon Calcarenite|69182|6|Mentioned|Chr p69, Ch3 p71|||||||Overlies the Toolonga Calcilutite. Overlain by the Giralia Calcarenite.||
9823|Korojon Calcarenite|69297|5|Briefly described|p249|Maastrichtian|Maastrichtian|Gascoyne Sub-basin of the Southern Carnarvon Basin. ||||Overlies the Toolonga Calcilutite. Unconformably overlain by the Miria Formation.|Calcarenite.|
9823|Korojon Calcarenite|70066|5|Briefly described|Regional: Fig.6|Maastrichtian|Maastrichtian|Exmouth and Barrow Sub-basins, Northern Carnarvon Basin.||||Overlies Toolonga Calcilutite and Withnell Formation. Is overlain by Miria Formation.||
9823|Korojon Calcarenite|70826|6|Mentioned|p7 tbl 4|Cretaceous|Cretaceous|Northern Carnarvon Basin.||||||
9823|Korojon Calcarenite|71790|6|Mentioned|p103|||Palynology p. 103.||||||
9823|Korojon Calcarenite|73564|6|Mentioned|p1225|Cretaceous|Cretaceous|Exmouth Plateau.||||Overlies Toolonga Calcilutite. Is overlain by Miria Formation. Equivalent to Withnell Formation.||
9896|Kulshill Group|7142|6|Mentioned|p350 Fig.4.|Early Permian|Late Carboniferous|Browse Basin. ||||Overlies Point Spring Sandstone. Is overlain by Fossil Head Formation.||
9896|Kulshill Group|13194|4|Described|p382, p388, p400, p405.|||See Table 4-16, Figs. 4-59 and 4-71. Maximum thickness below Petrel wells (up to 7km on seismic sections).||||Overlies Weaber Group.||
9896|Kulshill Group|13222|6|Mentioned|p229 Fig.2.||||||Includes Kuriyippi and Keyling Formations and Treachery Shale.|||
9896|Kulshill Group|13234|6|Mentioned|p250 Fig.2, p252 Fig.4, p256. |Permian|Carboniferous|||||Overlies Tanmurra Formation onshore.||
9896|Kulshill Group|13354|6|Mentioned|p375 Fig.6.|Early Permian|Late Carboniferous|Unit of Kinmore Group. Overlies Point Spring Sandstone and underlies Fossil Head Formation.||91||||28-OCT-14
9896|Kulshill Group|22663|5|Briefly described|NT97 -1-4 Fig.4|Permian|Carboniferous|||||||01-MAR-10
9896|Kulshill Group|24390|5|Briefly described|p2 Fig. 2, p3 Table 1|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
9896|Kulshill Group|24503|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Geological Province: Bonaparte Basin.||||||
9896|Kulshill Group|24569|5|Briefly described|p248 Fig. 3|Early Permian|Late Carboniferous|Includes the Keyling and Kuriyippi Formations and Treachery Shale. Geological Province: Petrel Sub-basin.||||||17-MAR-05
9896|Kulshill Group|41459|6|Mentioned|Fig.2|||See also Fig.4||||||
9896|Kulshill Group|41532|3|Fully described|p297|||||||||
9896|Kulshill Group|41689|6|Mentioned|Table 1|||||||||
9896|Kulshill Group|41690|4|Described|p5|||See also p74.||||||
9896|Kulshill Group|41731|5|Briefly described|p574|||||||||
9896|Kulshill Group|42055|5|Briefly described|p59|||||||||
9896|Kulshill Group|42056|5|Briefly described|p98|||||||||
9896|Kulshill Group|42075|5|Briefly described|Fig.4 P245|||||||||
9896|Kulshill Group|42150|6|Mentioned|p67|||||||||
9896|Kulshill Group|42442|3|Fully described|p13|||||||||
9896|Kulshill Group|43661|6|Mentioned|Fig.3|||||||||
9896|Kulshill Group|43699|6|Mentioned|Fig.6,p10||Permian|||||||
9896|Kulshill Group|49637|5|Briefly described|Fig.3|Early Permian|Late Carboniferous|Geological Province: Petrel Sub-basin.See also Fig. 6.||||||07-FEB-11
9896|Kulshill Group|50085|5|Briefly described|p2 Fig. 2, p3 Tb. 1|Permian|Permian|Age: <300Ma.  Geological Province: Bonaparte Basin.||||||
9896|Kulshill Group|60682|4|Described|p22 Table 5, 26|Early Permian|Late Carboniferous|Unconformably overlies Weaber Group. Sandstone, shale, siltstone, coal. Fluvial and fan delta with glacial influence. Geological Province: Bonaparte Basin.||||||
9896|Kulshill Group|61023|5|Briefly described|p2 Fig. 2|Permian|Permian|Geological Province: Bonaparte Basin.||||||10-APR-08
9896|Kulshill Group|61542|5|Briefly described|p277 Fig. 2|Stephanian|Westphalian|Includes Kuriyippi and Border Creek Formations - some uncertainty with latter unit 'parentage'? Overlies Wadeye Group. Geological Province: onshore Bonaparte Basin/Petrel-Sub-basin.||||||12-SEP-13
9896|Kulshill Group|62837|5|Briefly described|Stratigraphic columns|Early Permian|Namurian|Includes Kuriyippi Formation, Treachery Shale and Keyling Formation.  Age: ~311-~287Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
9896|Kulshill Group|63062|4|Described|p9 Fig. 9, p18|Early Permian|Late Carboniferous|Max. preserved thickness is in the Goulburn Graben: 5000m. Geological Province: Bonaparte Basin. Non-marine to marginal marine interbedded sandstone, siltstone and claystone, with minor coal and dolomitic rocks.||||||07-FEB-11
9896|Kulshill Group|64580|6|Mentioned|map legend|||||||||
9896|Kulshill Group|64630|5|Briefly described|p31 Fig.2, p37, p38|Artinskian|Sakmarian|Province: Bonaparte Basin. Underlies the Fossil Head Formation. Includes Keyling Formation, Treachery Shale and Kurriyippi Formation and onshore Keep Inlet Formation. Palynology age: P. confluens to D. byroensis.||||||24-NOV-09
9896|Kulshill Group|64694|6|Mentioned|p236, p242 Tb.4, p245 Fig.9|||Ruled out as source of oils in the Turtle field (Jefferies, 1988).||||Overlies Tanmurra Formation.||
9896|Kulshill Group|66949|6|Mentioned|p8|||Bonaparte Basin. Includes distinct glacial features in subsurface (core) sections, coeval with Reeves Formation.||||||
9896|Kulshill Group|67167|5|Briefly described|Map legend.|Permian|Permian||||||Undivided: friable feldspathic sandstone, siltstone, claystone; some diamictite and conglomerate.|
9896|Kulshill Group|67186|5|Briefly described|Map legend.|Permian|Permian||||||Friable feldspathic sandstone, siltstone, claystone; some diamictite and conglomerate.|23-NOV-11
9896|Kulshill Group|67354|5|Briefly described|p72, p73, pp88-92, pp100-108.|Permian|Late Carboniferous|Bonaparte Basin. Glacial deposits. Hosts oil and gas. Formerly part of the Port Keats Group. Seismic amplitude anomalies may be used as indicators of entrapped gas in sandstones in this Group.|||Offshore, includes Kuriyippi Formation at the base, Treachery Shale, and Keyling Formation at the top. Onshore, it also includes the Keep Inlet Formation.|Overlies the Wadeye Sub-Group.||
9896|Kulshill Group|69099|6|Mentioned|500k_geologyp08_lut.csv||||||Includes Keep Inlet Formation.|||31-JUL-15
9896|Kulshill Group|69165|6|Mentioned|500k_geologyp08_lut.csv|Permian|Permian||||Includes Keep Inlet Formation|||
9896|Kulshill Group|69297|5|Briefly described|p283, p285, p289, p290|Lower Permian|Upper Carboniferous|Bonaparte Basin. Up to 1500m thick in the Northern platform. Deposited in non-marine to marginal marine environments. Contains good to very good potential source rocks. Sandstones and mudstones are potential hydrocarbon reservoirs. |||||Interbedded sandstone, siltstone and claystone with minor coal and dolomitic rocks.|
9896|Kulshill Group|69451|5|Briefly described|p35:2-4, 8-11, 13-14|Permian|Late Carboniferous|Arafura Basin (offshore). These rocks in the Arafura Basin are referred to as Kulshill Group equivalent. Fluvial to marginal marine to shallow-marine deposits. 5000m thick in the Goulburn Graben; up to 3000m more is estimated to have been eroded in the Triassic. Most of the succession is Early Permian. There is a hiatus of c.45 m.y. following the Arafura Group, corresponding with the final phase of the Alice Springs Orogeny. Immature to mature for oil generation, depending on the thickness of Money Shoal Basin overburden. Contains good to very good petroleum source rocks. Reservoir potential is generally poor; multiple fracture sets could enhance the overall permeability and porosity. There may be intraformational seals.||||Unconformably overlies Arafura Group.|Interbedded sandstone, siltstone and claystone, with minor coal, and dolomitic rocks; palynoflora.|12-JUL-16
9896|Kulshill Group|69452|5|Briefly described|p36:4-5, 8-9, 11-12, 15, 17-19, 25-26|Permian|Late Carboniferous|Gunn (1988); equivalent to Kulshill Formation (Caye, 1968; Hughes, 1978). Petrel and Keep Inlet Sub-basins, Bonaparte Basin. Over 1500m thick. Glacial strata in the Basin are restricted to this Group. Minor coal has been reported.|||Keyling, Ditji, Quoin, Treachery, Border Creek, Keep Inlet, Kuriyippi Formations.|Unconformably overlies Wadeye Group or Langfield Group. Is overlain by Fossil Head Formation (Kinmore Group) unconformably to conformably.||12-JUL-16
9896|Kulshill Group|69454|5|Briefly described|p38:4|Cisuralian|Carboniferous|Petrel Sub-basin, Bonaparte Basin.|||Kuriyippi, Treachery, Quoin, Ditji and Keyling Formations.|Is overlain by Kinmore Group.||12-JUL-16
9896|Kulshill Group|69456|5|Briefly described|p40:2 Fig.40.3|Permian|Late Carboniferous|Arafura Basin. Referred to as "Kulshill Group equivalent".||||Overlies Arafura Group. Is overlain unconformably by Kulshill Group.||12-JUL-16
9896|Kulshill Group|69634|5|Briefly described|500k_geologyp08_lut.csv||||||Includes Keep Inlet Formation.|||
9896|Kulshill Group|69653|5|Briefly described|p10, 14-15|Permian|Carboniferous|Petrel Sub-basin. A sag-dominated regressive cycle.|||Kuriyippi, Treachery, Quoin, Ditji, Keyling Formations.|Overlies Wadeye Group. Is overlain by Kinmore Group.|Thick, shallow-marine, deltaic, and fluvial sediments.|
9896|Kulshill Group|69673|6|Mentioned|p166 fig 136, p167,  p172, p181, |Permian|Carboniferous|Over 1500m thick. Source rock potential in some units.|||Includes Kuriyippi Formation, Border Creek Formation, Treachery Formation, Quoin Formation, Ditji Formation, Keyling Formation, Keep Inlet Formation,|Unconformably overlain by Kinmore Group, overlies Weaber Group, unconformably overlies Wadeye Group||
9896|Kulshill Group|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3; p2|Sakmarian|Bashkirian|See also Regional geology: Fig.8, p8, p11. Permian marginal marine, fluvial and glacial reservoirs in this unit are proven hydrocarbon reservoirs. Intraformational seals occur in upper parts of this unit.|||Kuriyippi, Treachery, Quoin, Ditji and Keyling Formations.|Overlies Aquitaine Formation. Is overlain by Kinmore Group.||12-JUL-16
9896|Kulshill Group|70064|5|Briefly described|Regional Fig. 6|Sakmarian|Bashkirian|Caswell-Barcoo Sub-basins and Prudhoe Terrace, Browse Basin.||||Overlies Weaber Group. Is overlain by Kinmore Group.||12-JUL-16
9896|Kulshill Group|70098|4|Described|p5,p7-9, p18 Fig.4, p19 Fig.5, p22 Fig.8|Cisuralian|Mississippian|Bonaparte Basin. Kulshill Group equivalent, Permo-Carboniferous in Arafura Basin in Fig.4. Non-marine to marginal marine sediments unconformably overlying Arafura Group are approximately equivalent in age to the Kulshill Group. Significant oil shows in Mesozoic reservoirs were intersected. Potential source and reservoir rocks occur in Kulshill Group equivalent. Usually refers to a unit in text as Kulshill Group equivalent (Carboniferous-Permian) - not always clear if the actual or equivalent unit is being referred to.||||Overlies Darbilla Formation (Arafura Group). Is overlain by Plover Formation (Troughton Group).||
9896|Kulshill Group|70826|6|Mentioned|p6 tbl 3|Early Permian|Late Carboniferous|Southern Bonaparte Basin.||||||
9896|Kulshill Group|71146|5|Briefly described|p6,  p43 fig 33|Sakmarian|Late Carboniferous|Bonaparte Basin.|||||Mixed sandstone, mudstone and coal.|
9896|Kulshill Group|71267|4|Described|GEOL_LUT_CSV files|||Of Bonaparte Basin, Westralian Superbasin. Events: Timorese Collision (20-0.01 Ma); Gondwana breakup-northern NW Shelf (320-138 Ma); Outboard Bonaparte uplift/erosion (154-152 Ma); Alice Springs Orogeny (450-295 Ma); Eclipse Movement (340-300 Ma)See 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|||Includes Keep Inlet Formation.||Sandstone, siltstone, mudstone, conglomerate (including diamictite); minor limestone and coal; in part glacigene|
9896|Kulshill Group|72034|6|Mentioned|500k_interpgeop16_lut|Sakmarian|Asselian|Mentioned as parent unit. Age assumed from constituents. No other data.|||Includes Keep Inlet Formation.|||
9896|Kulshill Group|73083|6|Mentioned|p16|Triassic|Permian|||||||
9896|Kulshill Group|73117|6|Mentioned|p15, p32|Sakmarian|Bashkirian|Bonaparte Basin. Contains glacial facies similar to those in the Grant Group. Upper and lower portion of the constituent Kuriyippi Formation separated by a ?regional hiatus [~12 Myr?].|||Keyling Formation, Ditji Formation, Quoin Formation, Treachery Formation, Kuriyippi Formation.|Overlain by Fossil Head Formation.|Includes glacial facies.|
9896|Kulshill Group|73184|6|Mentioned|p201 Fig.12|Asselian|Asselian|Written as Kulshill Gp.||||||
9907|Kundip Quartzite|9173|5|Briefly described|Map legend.|Proterozoic|Proterozoic|||Unit in Mount Barren Group.|||Partially to completely recrystallised quartz arenite and micaceous sandstone.|27-AUG-13
9907|Kundip Quartzite|23727|4|Described|p72|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kybulup Schist. Underlying unit Steere Formation.||||||
9907|Kundip Quartzite|23728|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kybulup Schist. Underlying unit Steere Formation. Geological Province Albany-Fraser Orogen.||||||
9907|Kundip Quartzite|23752|4|Described|p14|Archean|Archean|Of Mount Barren Group. Overlying unit Kybulup Schist. Underlying unit Steere Formation.||||||07-NOV-08
9907|Kundip Quartzite|23753|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Barren Group. Quartzite, massive to coarsely bedded; minor pelitic beds. Geological Province: Albany-Fraser Orogen.||||||27-AUG-13
9907|Kundip Quartzite|23754|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Overlying unit Kybulup Schist. Underlying unit Steere Formation. Geological Province Albany-Fraser Orogen.||||||
9907|Kundip Quartzite|42424|5|Briefly described|p4|||||||||
9907|Kundip Quartzite|44137|5|Briefly described|p257|||Intruded by dolerite sills.||Mount Barren Group||||
9907|Kundip Quartzite|62381|5|Briefly described|p4-5, pp12-17.|||Type area 1 km north of Kundip. Cross-beds indicate sediment supply from the north.||Unit in Mount Barren Group.|||Well-bedded orthoquartzite with cross-bedding and local shale-rich horizons.|30-JUN-14
9907|Kundip Quartzite|63866|5|Briefly described|p187|||Albany-Fraser Belt. SHRIMP ages are derived from Nelson, 1997 and interpreted as the maximum depositional ages of the sedimentary protoliths to the quartzite.|1917 +/- 13 and 1851 +/- 30 Ma |Mount Barren Group|||Quartzite.|
9907|Kundip Quartzite|65487|4|Described|p22, 24|Paleoproterozoic|Paleoproterozoic|Of the Mount Barren Group. Thickly-bedded pure quartzite interbedded with mica- and magnetite-bearing quartzites and mudstone; minor thin lenses of metaconglomerate; common cross-bedding and ripple marks suggest shallow near shore marine to tidal sandflat conditions: delta-plain or upper delta-front.||||||10-FEB-14
9907|Kundip Quartzite|67268|6|Mentioned|p5|||||Mount Barren Group||||
9907|Kundip Quartzite|67722|6|Mentioned|p8|Statherian|Statherian|||Mount Barren Group||||
9907|Kundip Quartzite|68186|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Forms prominent rocky peaks. Deposition in shallow, near-shore marine to tidal-sandflat conditions.||Mount Barren Group.|||Predominantly thickly-bedded pure quartzite, interbedded with mica- and magnetite-bearing quartzite and mudstone, and minor thin lenses of metaconglomerate dominated by quartzite clasts. Sedimentary structures common.|
9907|Kundip Quartzite|69252|5|Briefly described|p10-11|||Delta plain or upper delta front sediments.||Mount Barren Group.||Overlies Steere Formation. Is overlain by Kybulup Schist.|Massive to coarsely-bedded orthoquartzite, interbedded with mica- and magnetite-bearing quartzites and mudstones.|
9907|Kundip Quartzite|69595|4|Described|p8, p10 tbl 2, p11, p13 fig 7a, p15, |Statherian|Statherian|Contains numerous sedimentary structures such as cross bedding and ripple marks suggesting deposition under a shallow, near-shore marine to tidal-sandflat conditions. Overlain by an unnamed 26m thick unnamed unit of thinly bedded, medium to coarse-grained sandstone and carbonaceous shale. Minimum 13m thick. See also  p36, p38, p57, p58.|1693 +/- 4 Ma|Mount Barren Group||Overlies the Steere Formation,|Thickly bedded pure quartzite which is interbedded with mica and magnetite-bearing quartzite and mudstone with minor thin lenses of metaconglomerate that is dominated by quartzite clasts.|
9907|Kundip Quartzite|70090|4|Described|p446,448,457|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton; also Yilgarn Craton. Of Barren Basin. Thickness: >13m. Depositional environment: Shallow, near-shore marine to tidal-sand flat conditions; delta-plain or upper delta-front. Deposited in a deepening rift basin, allowing marine incursions due to fault-controlled subsidence to occur at a greater rate than sedimentation. Metamorphosed to greenschist to amphibolite facies.||Unit of Mount Barren Group.||Overlain by Kybulup Schist. Underlain by Steere Formation.|Quartz-rich sandstone, mudstone, thin conglomerate.|
9907|Kundip Quartzite|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||quartzite, sandstone|
9908|Kungangie beds|45153|6|Mentioned|App.4-58|||||||||
9911|Kununurra Formation|13194|4|Described|p393 Tb.4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: 11km NNE Kununurra, 15o41'S 128o46'E. Zero to 105m thick shallow marine deposits.||||Overlies Kellys Knob Sandstone (conformably). Overlain by Abney Sandstone (conformably).|Quartz sandstone; minor dolomitic sandstone, and shale.|
9911|Kununurra Formation|40993|6|Mentioned|p4|||||||||
9911|Kununurra Formation|41864|3|Fully described|p51|||||||||
9911|Kununurra Formation|41865|5|Briefly described|Map legend|Frasnian||||||||
9911|Kununurra Formation|42030|5|Briefly described|p749|||||||||
9911|Kununurra Formation|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
9911|Kununurra Formation|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
9911|Kununurra Formation|69452|6|Mentioned|p36:6|Frasnian|Frasnian|||Cockatoo Group.||||12-JUL-16
9911|Kununurra Formation|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
9923|Kuriyippi Formation|12466|5|Briefly described|p177 Fig.10.|||||||Overlies Point Spring Sandstone. Is overlain by Treachery Shale.||03-SEP-14
9923|Kuriyippi Formation|13194|4|Described|p388 Tb. 4-16; p382, 405 figs 4-59,-71 |Asselian|Gzhelian|Type Section: Lesueur 1 well (1784-2801m). 19-1017m thick fluvial or tidal deposits with glacial floodplain towards top.||Kulshill Group||Overlies Point Spring Limestone. Overlain by Treachery Shale.|Silicified sandstone, tillite, conglomerate, shale; minor coal.|
9923|Kuriyippi Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kulshill Group.||||
9923|Kuriyippi Formation|13234|5|Briefly described|p250 Fig.2, p256.|Late Carboniferous|Late Carboniferous|Mis-spelt as Kuryippi Formation in Fig.2.|||||Includes sandstone.|
9923|Kuriyippi Formation|13354|6|Mentioned|p376 Fig.7.|Early Permian|Early Permian|Bonaparte Basin. Underlies Treachery Shale. Equivalent to part of Upper Grant Group of onshore Canning Basin.||109||||28-OCT-14
9923|Kuriyippi Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Carboniferous|Of the Kulshill Group.||||||01-MAR-10
9923|Kuriyippi Formation|23377|6|Mentioned|p212 Fig.5||Pennsylvanian|Of Vulcan Sub-basin.||||||09-OCT-06
9923|Kuriyippi Formation|24378|5|Briefly described|p14, p15|Late Carboniferous|Late Carboniferous|Geological Province: Bonaparte Basin.||||||
9923|Kuriyippi Formation|24569|5|Briefly described|p248 Fig. 3|Stephanian|Westphalian|Of the Kulshill Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
9923|Kuriyippi Formation|41459|6|Mentioned|Fig.2|||||||||
9923|Kuriyippi Formation|41532|2|Defined|p300|Early Permian|Late Carboniferous|||||||
9923|Kuriyippi Formation|41731|6|Mentioned|Fig.3|||||||||
9923|Kuriyippi Formation|42055|4|Described|Fig.1 P52|||||||||
9923|Kuriyippi Formation|42150|6|Mentioned|p65|||||||||
9923|Kuriyippi Formation|42442|3|Fully described|p15|Stephanian|Stephanian|Same unit as Kuriyippi Formation, WA.  Age latest Carboniferous.||||||09-OCT-06
9923|Kuriyippi Formation|43661|6|Mentioned|Fig.3|||||||||
9923|Kuriyippi Formation|60006|5|Briefly described|Map Legend|||Geological Province: Bonaparte Basin. Unconformably overlies Border Creek Member and Tanmurra Formation .||||||23-JUL-04
9923|Kuriyippi Formation|60386|5|Briefly described|p291, 297, p309|Sakmarian|Asselian|Petrel Sub-basin. Glacially influenced. Post-rift transition phase following Alice Springs Orogeny. Deltaic - nearshore - shelf. ||||Unconformably underlain by Point Spring Sandstone.|Glacial deposits.|
9923|Kuriyippi Formation|60682|5|Briefly described|p25 Fig. 22|Westphalian|Westphalian|Of Kulshill Group. Partially laterally equivalent to Keep Inlet Formation. Overlain by Treachery Shale. Shale. Geological Province: Bonaparte Basin.||||||09-OCT-06
9923|Kuriyippi Formation|60701|5|Briefly described|p12-13|Late Carboniferous|Late Carboniferous|Includes glacio-fluvial sands; containing some oil.  Geological Province: Bonaparte Basin.||||||13-JAN-05
9923|Kuriyippi Formation|61542|5|Briefly described|p277 Fig. 2|Westphalian|Westphalian|Of the Kulshill Group. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
9923|Kuriyippi Formation|62837|5|Briefly described|Stratigraphic columns|Stephanian|Namurian|Of the Kulshill Group. Age: ~311-~295Ma. Geological Province:  Western Bonaparte Basin, Northern Bonaparte Basin, Petrel Sub-basin (offshore).||||||01-MAR-10
9923|Kuriyippi Formation|64694|6|Mentioned|p231, p235 Fig.3., p240 Tb.2, p245 Fig.9|Late Carboniferous|Late Carboniferous|Two samples of oil-stained sandstones of this unit were analysed in this study.||||Overlies Point Spring Sandstone or Tanmurra Formation. Is overlain by Treachery Shale.||
9923|Kuriyippi Formation|65331|6|Mentioned|cross-section only|||||||||
9923|Kuriyippi Formation|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes light grey sandstone; light grey sandstone and dark grey siltstone, mottled/bioturbated; grey diamictite?|23-DEC-22
9923|Kuriyippi Formation|67200|5|Briefly described|app 2 p8||||||||Mottled/bioturbated sandstone and siltstone.|
9923|Kuriyippi Formation|67354|3|Fully described|p73, pp74-78, p103, p104, p108.|Asselian|Late Carboniferous|Named after Kuriyippi Hills. Type section is 1,784-2,801 m in Lesueur-1; this needs revision, and this study informally names the upper part the Blacktip Member (of the Treachery Formation). The upper part of this unit is probably equivalent to Keep Inlet and basal Quoin Formations. Mainly fluvial (meandering stream), and possibly shallow marine environment. Contains gas in Blacktip-1; several other wells have residual oil shows. Treachery Formation shales act as seals. An extensive network of channels is cut into the top of this unit; interpreted as glacial-related tunnel valleys. Between these are hills of possible gas-bearing sandstone.||Basal offshore unit in Kulshill Group.||Overlies the Wadeye Sub-Group. Is overlain unconformably by Treachery Formation.|A series of upward-fining cycles of sandstones with variable clay and carbonate cements, overlain by carbonaceous siltstone and shale; overlain by glacial strata; conglomerates common; local coal onshore.|
9923|Kuriyippi Formation|69451|6|Mentioned|p35:9|||Bonaparte Basin. Correlated with part of the Kulshill Group equivalent rocks in the Arafura Basin.||||||12-JUL-16
9923|Kuriyippi Formation|69452|3|Fully described|p36:9, 11-12, 15, 17-18|Permian|Late Carboniferous|Mory (1991). Petrel Sub-basin, Bonaparte Basin. Mainly fluvial deposits in lower part; glacigenic in upper part. Maximum thickness of 1017m in the type section in offshore drillhole Lesueur 1. Extensive unit, offshore and onshore. Bashkirian to Asselian age range. The glacigenic top of the Formation has been informally named the Blacktip member (of the Treachery Formation) by Gorter et al. (2008) [who in fact presented it as Blacktip Member].||Kulshill Group.||Unconformably overlies Aquitaine Formation (Wadeye Group). Is overlain unconformably by Treachery Formation. Equivalent to Border Creek Formation.|A thick succession of 30-90m-thick upward-fining cycles of sandstone and lesser amounts of siltstone, shale and minor coal, overlain by glacial sandstone and conglomerate.|12-JUL-16
9923|Kuriyippi Formation|69454|5|Briefly described|p38:4|Asselian|Carboniferous|Petrel Sub-basin, Bonaparte Basin.||Kulshill Group.||Correlated with Crown Point Formation (Pedirka Basin).||12-JUL-16
9923|Kuriyippi Formation|69653|6|Mentioned|p10|Cisuralian|Carboniferous|Petrel Sub-basin.||Kulshill Group.||Overlies Aquitaine Formation (Wadeye Group). Is overlain by Treachery Formation.||
9923|Kuriyippi Formation|69673|4|Described|p168 fig 138, p170 fig 142, p172|Permian|Carboniferous|Maximum thickness of 1017m. "Live" oil recorded in this unit.||Kulshill Group||Overlain by Treachery Formation, overlies Wadeye Group, Tanmurra Formation|Upwards fining cycles of sandstone, siltstone, shale and minor coal overlain by glacial sandstone and conglomerate.|
9923|Kuriyippi Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3, p3|Sakmarian|Bashkirian|See also Regional geology: Fig.8, p5, p11, p13. Hydrocarbon reservoir. Sealed by overlying Treachery Formation.||Kulshill Group.||Overlies Aquitaine Formation (Wadeye Group). Is overlain by Treachery Formation.|Glacial sediments.|12-JUL-16
9923|Kuriyippi Formation|70206|6|Mentioned|cross-section only|||Doubtfully identified as the unit overlying the Tanmurra Formation and Border Creek Member. Age not specified.||||||
9923|Kuriyippi Formation|72505|5|Briefly described|p890|Asselian|Carboniferous|Southern Bonaparte Basin. Correlated with the Microbaculispora tentula zone.||||Overlain by the Treachery Formation.||
9923|Kuriyippi Formation|73117|6|Mentioned|p15|Asselian|Bashkirian|Bonaparte Basin, southern. Upper and lower portion separated by a ?regional hiatus [~12 Myr?].||Kulshill Group||Overlain by Treachery Formation.||
9926|Kurramia Conglomerates|36869|6|Mentioned|p48|||||||||
9938|Kuruman Iron Formation|41997|6|Mentioned|p72|||||||||
9938|Kuruman Iron Formation|68141|6|Mentioned|p195|||Appears as Kuruman BIF.||||||
9967|Kybulup Schist|9173|5|Briefly described|Map legend.|Proterozoic|Proterozoic|||Unit in Mount Barren Group.|||Shale, sandstone, phyllite and schist; includes banded iron-formation: alternating layers of iron oxides and granoblastic quartz.|27-AUG-13
9967|Kybulup Schist|23727|4|Described|p73|Proterozoic|Proterozoic|Of Mount Barren Group. Underlying unit Kundip Quartzite.||||||
9967|Kybulup Schist|23728|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Underlying unit Kundip Quartzite. Geological Province Albany-Fraser Orogen.||||||
9967|Kybulup Schist|23752|4|Described|p15|Archean|Archean|Of Mount Barren Group. Underlying unit Kundip Quartzite.||||||07-NOV-08
9967|Kybulup Schist|23753|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Barren Group.  Pelitic schist and phyllite with minor psammitic layers.  Geological Province: Albany-Fraser Orogen.||||||26-MAY-04
9967|Kybulup Schist|23754|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Mount Barren Group. Underlying unit Kundip Quartzite. Geological Province Albany-Fraser Orogen.||||||
9967|Kybulup Schist|23808|5|Briefly described|p7|Neoproterozoic|Neoproterozoic|Of Mount Barren Group.  Geological Province: Yilgarn Craton.||||||
9967|Kybulup Schist|24165|6|Mentioned|p52, p57|Proterozoic|Proterozoic|Hosts the Hamersley Gorge (average grade 31.4% Mn) and Coppermine Creek (44% Mn) manganese deposits. Considered prospective for further Mn discoveries. A quartz vein in this unit hosts Pb minerals, 8km N of Bremer Bay.||||||
9967|Kybulup Schist|42424|5|Briefly described|p4|||Reserved R. Thom 1980, listed NLR.||||||
9967|Kybulup Schist|44137|5|Briefly described|p257|||Derived from pelitic and semi-pelitic rocks.||Mount Barren Group||||
9967|Kybulup Schist|62381|5|Briefly described|p4-5, pp13-18.|||Interbedded pelite and quartzite beds show multiple fold and cleavage generations.||Unit in Mount Barren Group.|||Amphibolite-facies psammitic to pelitic rocks. Cross-bedding common.|30-JUN-14
9967|Kybulup Schist|63866|5|Briefly described|p187|||Albany-Fraser Belt.||Mount Barren Group|||Psammitic and pelitic schists with subordinate dolomite and metaconglomerate.|
9967|Kybulup Schist|65487|5|Briefly described|p22, 24|Mesoproterozoic|Paleoproterozoic|Of the Mount Barren Group. Variably metamorphosed, thinly-bedded pelitic and psammitic rocks, rare dolomite and calc-silicate schist; increasing metamorphic grade towards the SE. Lower delta-front, possibly with an upper prograding section. A 26m thick xenotime-bearing phosphatic unit between the Kundip Quartzite and this unit has been dated: 1693 +/- 4 Ma (Vallini et al., 2005).||||||10-FEB-14
9967|Kybulup Schist|67268|6|Mentioned|p5|||||Mount Barren Group||||
9967|Kybulup Schist|67722|6|Mentioned|p8|Statherian|Statherian|||Mount Barren Group||||
9967|Kybulup Schist|68186|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|||Mount Barren Group.||Is intruded by Cowerdup Sill.|Predominantly thinly bedded pelitic and psammitic rocks with variable metamorphic grade. In the NW, mainly slate and phyllite with rhythmite and shale coarsening-upwards into siltstone. In the SE, kyanite-, staurolite- and garnet-bearing schists.|
9967|Kybulup Schist|69252|5|Briefly described|p10-11|||Lower delta front deposits.|1693 +/- 4 Ma (diagenetic xenotime).|Mount Barren Group.||Overlies Kundip Quartzite.|Thinly bedded pelitic and psammitic rocks of variable metamorphic grade.|
9967|Kybulup Schist|69595|4|Described|p8, p9 fig 5, p10 tbl 2, p11.|Statherian|Statherian|Yilgarn Craton, Barren Basin, Biranup Zone. Deposited in marine setting that includes carbonate banks surrounded by deeper water. Minimum 35m thick. Underlain by an unnamed 26m thick unnamed unit of thinly bedded, medium to coarse-grained sandstone and carbonaceous shale. See also p13 fig 7a, p15, p36, p58.|1751 +/- 19 - 1693 +/- 4 Ma (depositional age)|Mount Barren Group|||Slate, phyllite, mudstone-dominant rythmite and shale that coarsens upwards into siltstone. Amphibolite facies kyanite, stuarolite and garnet bearing schists is dominant in places. Rare outcrops of dolostone and calc-silicate schist also occur.|
9967|Kybulup Schist|70090|4|Described|p446,448|Statherian|Statherian|Geological province: Biranup Zone, Albany-Fraser Orogen, West Australian Craton; also Yilgarn Craton. Of Barren Basin. Thickness: >35m. Depositional environment: Carbonate banks surrounded by deeper-water sediments; lower delta-front. Metamorphosed to greenschist to amphibolite facies.||Unit of Mount Barren Group.||Underlain by Kundip Quartzite.|Thinly-bedded pelitic and psammitic rocks and sparse dolostone and calc-silicate schist.|
9967|Kybulup Schist|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||shale, sandstone, phyllite, siltstone|
10000|Lady Bountiful granite|42156|6|Mentioned|p373|||||||||
